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
27073|ABC Range Quartzite|1242|14|Not recorded|p9, 10, 11|||Underlain by Brachina Formation.||||||
27073|ABC Range Quartzite|7931|5|Briefly described|p98, p99 Fig. 2|Ediacaran|Ediacaran|Of Sandison Subgroup (Wilpena Group). Overlain by the Wilco "formation" sandy member at the base of the Bunyeroo Formation. Prograding shallow marine sands.||||||07-FEB-11
27073|ABC Range Quartzite|22921|6|Mentioned|37|||Parent Wilpena Group||||||
27073|ABC Range Quartzite|23180|6|Mentioned|p35|||||||||
27073|ABC Range Quartzite|23211|5|Briefly described|p40-42,44-46 Fig.2|||of Sandison Subgroup.||||||
27073|ABC Range Quartzite|23250|5|Briefly described|p1124 Fig.2||Neoproterozoic III|Of Wilpena Group. Correlate of Tent Hill Formation and Pertatataka Formation.||||||13-FEB-08
27073|ABC Range Quartzite|23287|6|Mentioned|p104 Fig.2-4|||Age: Lower Ediacarian. Adelaide Geosyncline.||||||
27073|ABC Range Quartzite|23719|5|Briefly described|p25 Taable 7|||See also page 26. Of Wilpena Group. O'lying unit Kulpara Limestone. U'lying unit Brachina Formation. Geological Province: Gawler Craton.||||||
27073|ABC Range Quartzite|23806|5|Briefly described|p1122 Fig. 1|Neoproterozoic|Neoproterozoic|||||||
27073|ABC Range Quartzite|23818|4|Described|p73 Fig.27, p75|Adelaidean|Adelaidean|Of the Wilpena Group. Overlain by Bunyeroo Formation. Underlain by Brachina Formation. Max. thickness: 2500 ft.||||||24-JUN-09
27073|ABC Range Quartzite|23913|4|Described|p110 Fig. 2|Adelaidean|Adelaidean|Geological Province: Central Flinders Zone. Of the Wilpena Group. Underlain by Brachina Formation. Overlain by Bunyeroo Formation.||||||24-JUN-09
27073|ABC Range Quartzite|23981|5|Briefly described|p10 Fig. 5, p25|Neoproterozoic|Neoproterozoic|Thin, planar-tabular bed sets with scoured bases- of fine-grained arkosic sst. with pebbly, phosphatised base and bioturbated pyritic siltstone top. Disconformable beneath Mount Terrible Fm. (basal unit of Normanville Gp). Geol. Prov: Stansbury Basin.||||||
27073|ABC Range Quartzite|24138|5|Briefly described|p10 Fig. 1.1|Precambrian|Precambrian|Ripples and current-bedding indicate a shallow water depositional environment. Geological Province: Adelaide Geosyncline.||||||
27073|ABC Range Quartzite|24175|5|Briefly described|p14|Neoproterozoic|Neoproterozoic|Of the Wilpena Group.  Max. thickness: ~1000m.||||||
27073|ABC Range Quartzite|24176|4|Described|p14, p24 Tb. 1|Adelaidean|Adelaidean|Of the Wilpena Group. Quartzite, sandstone. Overlain by Bunyeroo Formation; intertongues with Brachina Formation. Age is Marinoan. Max. thickness: 150m. Geological Province: Mount Painter Province.||||||13-FEB-08
27073|ABC Range Quartzite|24195|5|Briefly described|p45 Fig.3|Late Precambrian|Early Precambrian|Of the Sandison Subgroup. Geological Province: Adelaide Geosyncline.||||||13-FEB-08
27073|ABC Range Quartzite|24321|5|Briefly described|Map legend|Late Adelaidean|Late Adelaidean|Parent: Wilpena Group||||||
27073|ABC Range Quartzite|24476|4|Described|p547 Fig. 4|Vendian|Vendian|Overlies the Brachina Formation. Overlain by the Bunyeroo Formation. Geological Province: Adelaide fold belt.||||||
27073|ABC Range Quartzite|24546|5|Briefly described|p2 - 3 Fig.2|Neoproterozoic|Neoproterozoic|Of Wilpena Group. Geological Province: Adelaide Fold Belt.||||||16-JAN-08
27073|ABC Range Quartzite|24586|5|Briefly described|p51 Fig. 2|Adelaidean|Adelaidean|Of the Sandison Subgroup (Wilpena Group, Heysen Supergroup). Geological Province: Adelaide Geosyncline.  See also p52 Fig. 3.||||||03-APR-13
27073|ABC Range Quartzite|29780|5|Briefly described|p45|||||||||
27073|ABC Range Quartzite|29781|5|Briefly described|p45|||||||||
27073|ABC Range Quartzite|30176|6|Mentioned|Map legend|Adelaidean|Adelaidean|Marinoan||||||
27073|ABC Range Quartzite|30198|4|Described|p96|||||||||
27073|ABC Range Quartzite|30800|6|Mentioned|p220|||On Fig.1.||||||
27073|ABC Range Quartzite|30801|6|Mentioned|p5|||See also P6. Table. Marinoan age.||||||
27073|ABC Range Quartzite|30802|6|Mentioned|p5|||Marinoan age||||||
27073|ABC Range Quartzite|30807|6|Mentioned|p102|||Suggested mapping symbol||||||
27073|ABC Range Quartzite|31923|6|Mentioned|p10|||Adelaidean. U. Wilpena Gp.||||||
27073|ABC Range Quartzite|32146|6|Mentioned|Fig.3|||||||||
27073|ABC Range Quartzite|32504|6|Mentioned|Fig.2|||||||||
27073|ABC Range Quartzite|32505|6|Mentioned|Table 3|||||||||
27073|ABC Range Quartzite|32506|6|Mentioned|Fig.1|||||||||
27073|ABC Range Quartzite|32511|6|Mentioned|Fig.1|||||||||
27073|ABC Range Quartzite|32720|6|Mentioned|Table 1|||||||||
27073|ABC Range Quartzite|32722|6|Mentioned|Fig.3|||Stromatolite. Adelaidean||||||13-JAN-11
27073|ABC Range Quartzite|32724|6|Mentioned|Fig.1|||Correlation. Marinoan||||||
27073|ABC Range Quartzite|33036|6|Mentioned|Fig.2|||||||||
27073|ABC Range Quartzite|33037|6|Mentioned|Fig.2|||||||||
27073|ABC Range Quartzite|33474|6|Mentioned|Fig.3|||||||||
27073|ABC Range Quartzite|33934|6|Mentioned|p2398|||||||||
27073|ABC Range Quartzite|34116|6|Mentioned|p19|||||||||
27073|ABC Range Quartzite|34267|6|Mentioned|Fig.|||The Oraparinna and Enorama diapiric structures.||||||
27073|ABC Range Quartzite|34269|6|Mentioned|Table 1|||U.Prot.||||||
27073|ABC Range Quartzite|34291|5|Briefly described|p20|||Adelaidean. See also PP21,44,52 etc||||||
27073|ABC Range Quartzite|34521|5|Briefly described|p156|||Suitability for road-making||||||
27073|ABC Range Quartzite|34535|4|Described|p75|||See also Fig.27||||||
27073|ABC Range Quartzite|34835|6|Mentioned|Fig.2|||||||||
27073|ABC Range Quartzite|34836|6|Mentioned|Fig.2|||||||||
27073|ABC Range Quartzite|34844|6|Mentioned|Fig.2|||||||||
27073|ABC Range Quartzite|34901|6|Mentioned|p18|||||||||
27073|ABC Range Quartzite|35075|6|Mentioned|Fig.2|||||||||
27073|ABC Range Quartzite|35143|6|Mentioned|Fig.2|||||||||
27073|ABC Range Quartzite|35158|6|Mentioned|p47|||||||||
27073|ABC Range Quartzite|35195|6|Mentioned|Table 3|||||||||
27073|ABC Range Quartzite|35255|5|Briefly described|p11|||See also Fig.4.||||||
27073|ABC Range Quartzite|35582|6|Mentioned|Fig.2|||||||||
27073|ABC Range Quartzite|35586|1|Redefined|p30|late Adelaidean|late Adelaidean|Definition of Dalgarno and Johnson 1964 retained and expanded.||||||20-FEB-08
27073|ABC Range Quartzite|35678|6|Mentioned|Fig.2|||Geological cross-sections, northern Yorke Peninsula.||||||
27073|ABC Range Quartzite|35798|6|Mentioned|Fig.4|||Correlation of lower units in Desert Syncline drill holes.||||||
27073|ABC Range Quartzite|36212|6|Mentioned|Fig.3|||||||||
27073|ABC Range Quartzite|36244|6|Mentioned|p2|||Redefined by Plummer 1978.||||||
27073|ABC Range Quartzite|36621|6|Mentioned|Fig.1|||||||||
27073|ABC Range Quartzite|36622|6|Mentioned|Fig.2|||||||||
27073|ABC Range Quartzite|36731|6|Mentioned|p124|||||||||
27073|ABC Range Quartzite|36898|6|Mentioned|p197|||||||||
27073|ABC Range Quartzite|37461|6|Mentioned|Fig.5.11|||||||||
27073|ABC Range Quartzite|37627|6|Mentioned|p188|||||||||
27073|ABC Range Quartzite|38022|6|Mentioned|Fig.4|||||||||
27073|ABC Range Quartzite|38157|6|Mentioned|Table V|||||||||
27073|ABC Range Quartzite|38970|6|Mentioned|Fig.15|||||||||
27073|ABC Range Quartzite|39210|6|Mentioned|Table 4|||||||||
27073|ABC Range Quartzite|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Marinoan||||||
27073|ABC Range Quartzite|39351|6|Mentioned|Map legend|Adelaidean|Adelaidean|Marinoan||||||
27073|ABC Range Quartzite|39352|6|Mentioned|Map legend|Adelaidean|Adelaidean|Marinoan||||||
27073|ABC Range Quartzite|39490|6|Mentioned|Fig.1(6)|||||||||
27073|ABC Range Quartzite|39675|6|Mentioned|Fig.2|||||||||
27073|ABC Range Quartzite|39807|6|Mentioned|p225|||||||||
27073|ABC Range Quartzite|39808|6|Mentioned|p223|||||||||
27073|ABC Range Quartzite|40442|6|Mentioned|Fig.4|||||||||
27073|ABC Range Quartzite|40455|5|Briefly described|p75|||||||||
27073|ABC Range Quartzite|40456|4|Described|p28|||||||||
27073|ABC Range Quartzite|40720|5|Briefly described|p55|||||||||
27073|ABC Range Quartzite|41005|6|Mentioned|p418|||||||||
27073|ABC Range Quartzite|41236|5|Briefly described|p63|||||||||
27073|ABC Range Quartzite|41429|3|Fully described|p225|||||||||
27073|ABC Range Quartzite|41496|6|Mentioned|Fig.1|||||||||
27073|ABC Range Quartzite|41794|6|Mentioned|p790|||||||||
27073|ABC Range Quartzite|41801|6|Mentioned|Fig.4|||||||||
27073|ABC Range Quartzite|41833|6|Mentioned|p586|||||||||
27073|ABC Range Quartzite|41953|6|Mentioned|Fig.2 P133|||||||||
27073|ABC Range Quartzite|42028|6|Mentioned|p137|||||||||
27073|ABC Range Quartzite|42095|5|Briefly described|p30|||See also Fig.3||||||
27073|ABC Range Quartzite|42098|5|Briefly described|Table 2 p54|||||||||12-JUL-16
27073|ABC Range Quartzite|42222|6|Mentioned|p18|||||||||
27073|ABC Range Quartzite|42225|6|Mentioned|p219|||||||||
27073|ABC Range Quartzite|42235|4|Described|p141|||See also Fig.3||||||
27073|ABC Range Quartzite|42238|5|Briefly described|p77|||||||||
27073|ABC Range Quartzite|42239|6|Mentioned|Fig.2 P151|||||||||
27073|ABC Range Quartzite|42240|6|Mentioned|p166|||||||||
27073|ABC Range Quartzite|42241|5|Briefly described|p178|||||||||
27073|ABC Range Quartzite|42243|5|Briefly described|p209|||||||||
27073|ABC Range Quartzite|42272|5|Briefly described|p403|||||||||
27073|ABC Range Quartzite|42498|5|Briefly described|Map Legend|Adelaidean|Adelaidean|||||||
27073|ABC Range Quartzite|42505|5|Briefly described|Map legend|Adelaidean (Marinoan)||||||||
27073|ABC Range Quartzite|42546|5|Briefly described|Map legend|Adelaidean (Marinoan)||||||||
27073|ABC Range Quartzite|42600|5|Briefly described|p10|||||||||
27073|ABC Range Quartzite|42736|5|Briefly described|map legend|Neoproterozoic||||||||
27073|ABC Range Quartzite|42763|5|Briefly described|Fig.3 p23|||||||||12-JUL-16
27073|ABC Range Quartzite|42813|6|Mentioned|p22|||of Wilpena Group||||||
27073|ABC Range Quartzite|42821|6|Mentioned|p137|||||||||
27073|ABC Range Quartzite|42882|6|Mentioned|p11|||||||||
27073|ABC Range Quartzite|43052|5|Briefly described|p192, table 6.1|||Of Wilpena  Group.||||||12-JUL-16
27073|ABC Range Quartzite|43053|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Deltaic sandstone.||||||26-MAY-05
27073|ABC Range Quartzite|43094|6|Mentioned|p36|||||||||
27073|ABC Range Quartzite|43258|5|Briefly described|Map Legend||Neoproterozoic|||||||
27073|ABC Range Quartzite|43298|5|Briefly described|Map Legend||Adelaidean|||||||
27073|ABC Range Quartzite|43595|5|Briefly described|p547|||||||||
27073|ABC Range Quartzite|43622|5|Briefly described|p37-39|Neoproterozoic||||||||
27073|ABC Range Quartzite|43650|6|Mentioned|p444|||||||||
27073|ABC Range Quartzite|43845|5|Briefly described|Fig3, p43, 46||Neoproterozoic|In Wilpena Group.||||||12-JUL-16
27073|ABC Range Quartzite|44934|5|Briefly described|Map Legend||Adelaidean|||||||
27073|ABC Range Quartzite|46865|6|Mentioned|Table 2|||||||||
27073|ABC Range Quartzite|50127|6|Mentioned|p48 Fig.2|||Geological Province: Stuart Shelf.||||||
27073|ABC Range Quartzite|60718|5|Briefly described|p49 Fig. 2|Adelaidean|Adelaidean|Geological Province: Adelaide Geosyncline.||Of Sandison Subgroup (Wilpena Group).||||15-APR-11
27073|ABC Range Quartzite|60953|5|Briefly described|Map Legend|Adelaidean|Adelaidean|||||||
27073|ABC Range Quartzite|60955|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Equivalent to Arcoona Quartzite Member. Of the Wilpena Group. Flaggy red-brown and purple sandstone-quartzites.||||||13-APR-05
27073|ABC Range Quartzite|60959|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Of the Sandison Subgroup. White, heavy-mineral laminated, cross bedded quartzite with ripple marks, mudcracks and mud clasts. Capped by orthoquartzite.||||||
27073|ABC Range Quartzite|61108|5|Briefly described|map legend|Adelaidean|Adelaidean|Deltaic sandstone.||||||
27073|ABC Range Quartzite|61236|6|Mentioned|p24 Fig. 1|Adelaidean|Adelaidean|||||||
27073|ABC Range Quartzite|61308|5|Briefly described|p7|Proterozoic|Proterozoic|||||||
27073|ABC Range Quartzite|61565|5|Briefly described|p609 Fig. 3|Neoproterozoic III|Neoproterozoic III|Geological Province: Adelaide Fold Belt.||||||
27073|ABC Range Quartzite|61732|3|Fully described|p5 Tb. 1, p43-44|||Previously Tent Hill Fm. Of Sandison Subgroup. Conformable over Brachina Fm. Geol.Prov: Adelaide Rift Complex. Lateral equivalent of ABC Quartzite, Simmens (Arcoola) Quartzite Member (Tent Hill Fm). See also p97.||||||13-MAY-16
27073|ABC Range Quartzite|62085|6|Mentioned|p19 Fig.4|Ediacaran|Ediacaran|||Wilpena Group|||Quartzite.|
27073|ABC Range Quartzite|62592|5|Briefly described|p50 Table 5.1.|Ediacaran|Ediacaran|Adelaide Geosyncline.||Unit in Sandison Subgroup.||Overlies Brachina Formation.|Quartzite, sandstone.|
27073|ABC Range Quartzite|62903|6|Mentioned|p730 Fig.1|||Adelaide Rift Complex. Presented in figure as ABC.||||overlies Brachina Formation; is overlain by Bunyeroo Formation||
27073|ABC Range Quartzite|63458|6|Mentioned|p897 Fig.19, |Ediacaran|Ediacaran|||Unit in Wilpena Group.||||
27073|ABC Range Quartzite|63811|6|Mentioned|p503|Ediacaran|Ediacaran|Stuart Shelf.||Of Wilpena Group.||||28-MAR-12
27073|ABC Range Quartzite|64455|5|Briefly described|p138 Fig. 1|Neoproterozoic III|Neoproterozoic III|Of Sandison Subgroup. Underlain by Brachina Formation. Crossbedded feldspathic sandstone. Age is Ediacaran.||||||
27073|ABC Range Quartzite|64797|6|Mentioned|p153 Fig.2, p164 Fig.11, p169 Fig.12|Ediacaran|Ediacaran|Adelaide Rift Complex. Lithology/rank not shown on diagram.||||||
27073|ABC Range Quartzite|64829|5|Briefly described|p1084 Fig. 1|Neoproterozoic|Neoproterozoic|||||||07-FEB-11
27073|ABC Range Quartzite|65313|6|Mentioned|p576 Fig. 5|Neoproterozoic|Neoproterozoic|||||||
27073|ABC Range Quartzite|65376|6|Mentioned|p140 Fig.4.22.|Neoproterozoic|Neoproterozoic|||||||
27073|ABC Range Quartzite|65410|6|Mentioned|p74.|||Adelaide Geosyncline. Part of Supersequence 3.||||||
27073|ABC Range Quartzite|65892|4|Described|p25, p32-33, p35, p38-39.  |Ediacaran|Ediacaran|Flinders Ranges, Adelaide Geosyncline. Forms prominent outcrops. Locally has mud cracks, ripple marks, clay pellets and load casts. Contains megascopic carbonaceous Chuaria-Tawuia acritarch assemblage.|c.590 Ma.|Unit in Wilpena Group.||Overlies Brachina Formation. Is overlain by Bunyeroo Formation.|Cross-bedded, well-sorted, fine- to medium-grained feldspathic sandstone.|
27073|ABC Range Quartzite|66569|5|Briefly described|p860, p861 fig.2,|Ediacaran|Ediacaran|Of Wilpena Group; deltaic and shallow marine; underlies Bunyeroo Formation; overlies Brachina Formation.||||||
27073|ABC Range Quartzite|67484|6|Mentioned|p294 Tb.1|Ediacaran|Ediacaran|Adelaide Rift Complex.||Of the Wilpena Group.||Overlain by Bunyeroo Formation. Underlain by Brachina Formation.||
27073|ABC Range Quartzite|67620|5|Briefly described|p5|Ediacaran|Ediacaran|Adelaide Rift Complex.||Wilpena Group.||Overlies Brachina Formation. Is overlain by Bunyeroo Formation.||
27073|ABC Range Quartzite|68030|4|Described|p237-239|Ediacaran|Ediacaran|Flinders Ranges. Also referred to as ABC Range Formation on p238. Up to 2km thick, and thins to the N and S to <100m (Plummer et al., 1990). Upward-shoaling Brachina Fm and ABC Range Qtz represent a HST of progradatioal siliciclastics from Gawler Craton into Andelaide Geosyncline.||Unit of Wilpena Group.||Overlain by Bunyeroo Formation, and infilled locally by Wilcolo Sandstone Member. Underlain/grades downwards into Brachina Formation.|Medium to thickly bedded sandstone with herringbone cross bedding and desiccation cracks.|
27073|ABC Range Quartzite|68138|6|Mentioned|p156|Neoproterozoic|Neoproterozoic|Adelaide Rift Complex.||Wilpena Group.||||
27073|ABC Range Quartzite|68269|6|Mentioned|p673-674|||Adelaide Geosyncline.||Wilpena Group||Underlain by Brachina Formation. Overlain by Bunyeroo Formation.|Sandstone dominated.|
27073|ABC Range Quartzite|68276|6|Mentioned|p73|||||||Shales, siltstones and sandstones overlie cap dolostones.||
27073|ABC Range Quartzite|68473|6|Mentioned|p531|||Adelaide Rift Complex.||||||
27073|ABC Range Quartzite|69019|3|Fully described|p54, p56.|Neoproterozoic|Neoproterozoic|Name first used by Mawson (1939); formalised by Dalgarno and Johnson (in Thomson et al., 1964). 120 m thick in their Wilpena Group stratotype section in Brachina Gorge.||Unit in Sandison Subgroup.||Is overlain unconformably by Bunyeroo Formation.|Pale pinkish-grey, slightly feldspathic quartzite (>90% quartz), fine- to medium-grained; minor greenish siltstone beds; scattered clay intraclasts; flaggy to medium-bedded; contains heavy mineral laminations.|
27073|ABC Range Quartzite|69666|6|Mentioned|p27 Fig.3|Neoproterozoic|Neoproterozoic|||||||
27073|ABC Range Quartzite|70031|5|Briefly described|p245|Ediacaran|Ediacaran|Adelaide Geosyncline. ||Unit of Wilpena Group.||Overlain by Bunyeroo Formation. Underlain by Brachina Formation.||
27073|ABC Range Quartzite|70082|6|Mentioned|p2|Ediacaran|Ediacaran|Flinders Ranges.||||||
27073|ABC Range Quartzite|70333|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic||||||Quartzite, slightly feldspathic, fine- to medium-grained, pale pinkish grey, clay intraclasts, flaggy to medium-bedded, heavy mineral lamination, minor siltstone.|
27073|ABC Range Quartzite|70334|4|Described|p2,20,33-37,57,66, 68,77-79,92|Ediacaran|Ediacaran|Geological province: Gawler Craton. Of Adelaide Geosyncline. Highstand systems tract, representing rapid marine transgression during interglacial period after Sturtian glaciation. Clean sands deposited as a continuous sheet over the Stuart Shelf and Adelaide Geosyncline. Thickness variation is a result of reactivation of the Torrens Hinge Zone, resulting in rapid increase in thickness on the eastern side of faults. Deeply incised, forming major canyons. Two main hypotheses for canyon incision: a) canyons cut by fluvial processes following base level change produced by tectonic uplift or Messinian-style sea level change and filled by coastal onlap, or b)  cut in an entirely marine environment (see p37,78 for details). Forms prominent ridges and hills in outcrop. Deposited in a very shallow marine to tidal flat environment, with some periods of subaerial exposure (Plummer, 1978; Preiss, 1987).||Unit of Sandison Subgroup.||Underlain by Brachina Formation.  Equivalent to Tent Hill Formation.|White, grey and pink fine- to medium-grained feldspathic to very clean quartzite.|14-OCT-19
27073|ABC Range Quartzite|70406|4|Described|p126, p124, 125, 127,128, 117|Neoproterozoic|Neoproterozoic|||Of Sandison Subgroup.||Overlain by Wilcolo Sandstone. In part equivalent to Corraberra Sandstone Member, Simmens Quartzite.|Pale pinkish grey to greyish white, thick-bedded to massive, fine to medium-grained, slightly feldspathic quartzite and minor interbedded shale and fine-grained sandstone. Various types of cross-bedding. Over 90% quartz.|29-APR-16
27073|ABC Range Quartzite|70407|5|Briefly described|p103 Fig 2, p101, 105, 106|Neoproterozoic|Neoproterozoic|Age: Marinoan.||Of Sandison Subgroup, Wilpena Group.||Disconformably overlain by Wilcolo Sandstone.||
27073|ABC Range Quartzite|70790|6|Mentioned|p258 Fig.1|Ediacaran|Ediacaran|Adelaide Rift Complex.||||||
27073|ABC Range Quartzite|71129|4|Described|p15,128,131|Ediacaran|Ediacaran|Of Adelaide Geosyncline. Deposited during rapid marine transgression.||Unit of Sandison Subgroup.||Broadly equivalent to Tent Hill Formation; partially equivalent to Simmens Quartzite Member/Tent Hill Fm..||
27073|ABC Range Quartzite|71237|14|Not recorded|p10|||||||||
27073|ABC Range Quartzite|71241|2|Defined|p13, 14, p9-10|||Of Mawson 1939.||Of Wilpena Group.||||
27073|ABC Range Quartzite|71242|14|Not recorded|p9,10,11|||Underlain by Brachina Formation. Also shown as A.B.C. Range Quartzite p10.||||||
27073|ABC Range Quartzite|71250|6|Mentioned|p70|Ediacaran|Ediacaran|Central Flinders Ranges.||Wilpena Group.||Overlies Brachina Formation. Is overlain by Bunyeroo Formation.||
27073|ABC Range Quartzite|72449|5|Briefly described|p1, p2 Map Legend|Neoproterozoic|Neoproterozoic|Beach sand.||||Overlies Brachina Formation and underlies Bunyeroo Formation.|White, heavy mineral laminated cross-bedded quartzite with ripple marks and mud-clasts.|
27073|ABC Range Quartzite|72450|5|Briefly described|Brochure, Brochure map|||Forms prominent outcrops at Ochre Point and on Willunga Scarp. Deformed by the Delamerian Orogeny.||Wilpena Group||Overlies the Brachina Formation. Underlies the Normanville Group.|Massive, hard quartzite.|
27073|ABC Range Quartzite|72451|6|Mentioned|p4 |||See also ABC Range quartzite, ABC range Quartzite, all p4, and used apparently interchangeably.||||Underlies Bunyeroo Formation.||
27073|ABC Range Quartzite|72456|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Marree 1:250k map sheet. |||||Quartzite, slightly feldspathic, fine to medium grained, pale pinkish grey, clay intraclasts, flaggy to medium bedded, heavy mineral lamination, minor siltstone.|
27073|ABC Range Quartzite|73086|6|Mentioned|p122, p130|||Adelaide Rift Complex.||||Correlates to Pertatataka Formation.||
27073|ABC Range Quartzite|73110|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic||||||Quartzite, slightly feldspathic, fine- to medium-grained, pale pinkish-grey, clay intraclasts, flaggy to medium-bedded, heavy mineral lamination, minor siltstone.|
27073|ABC Range Quartzite|73188|5|Briefly described|[See comments]|Ediacaran|Ediacaran|Mount Lofty Ranges. A comparatively more resistant rock type that composes Mount Barker. p: 308, 311, 315-316, 326, 331, 334-335, 343, 346, 356.||Sandison Subgroup, Wilpena Group||Disconformably overlain by Normanville Group. Unconformably overlain by Ochre Cove Formation.|Cross-bedded quartzite.|
27073|ABC Range Quartzite|73222|6|Mentioned|p11, p16, p24, p26|Ediacaran|Ediacaran|Adelaide Rift Complex.||Sandison Subgroup, Wilpena Group, Heysen Supergroup||||
27073|ABC Range Quartzite|73236|4|Described|p36-38, p40-41, p47|Ediacaran|Ediacaran|Marine-deltaic sedimentary rocks. Crops out at O'Sullivan Beach, south of Hallett Cove. Caps the Sandison Subgroup's upward-shallowing succession.||Sandison Subgroup, Wilpena Group, Heysen Supergroup||Underlain by Brachina Formation. Overlain by Bunyeroo Formation.|White, medium-grained, well-sorted, highly siliceous. cross-bedded quartzite.|
27073|ABC Range Quartzite|74367|5|Briefly described|p7 Fig.6, p8-9, p11, p14, p16-17, p22|Ediacaran|Ediacaran|MDA is likely within uncertainty of the true depositional age. See also p20.|630+/-16 Ma LA-ICP-MS detrital zircon MDA|Sandison Subgroup||||
39172|Aagot Member|24475|2|Defined|p52|Paleoproterozoic|Paleoproterozoic|Of Wandearah Foramtion. Overlain by Winulta Formation.||||||07-NOV-08
39172|Aagot Member|60958|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Wandearah Formation. Metasandstone-dominated unit. Metasandstone, sandy argillite, minor conglomerate, calc-silicate and albitic rocks. Geological Province: Gawler Craton.||||||07-NOV-08
39172|Aagot Member|61121|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Wandearah Formation. Layered metasandstone, sandy argillite, minor conglomerate, calcsilicate and albitic rocks; sandstone with haematite-coated grains, cross-bedding and heavy mineral banding. Age: ~1756Ma. Geological Province: Gawler Craton.||||||07-NOV-08
39172|Aagot Member|63398|5|Briefly described|p666|||Of the Wandearah Formation. Scapolite-bearing metasandstone and conglomerate. Intruded by Curramulka Gabbronorite. ||||||
39172|Aagot Member|65375|4|Described|pp19-21, p46.|Paleoproterozoic|Paleoproterozoic|Locally interbedded with felsic (Wardang Volcanics) volcanic rocks. Metamorphosed to lower amphibolite grade. A fluvial-aeolian to foreshore environment is suggested.||Unit in Wandearah Formation.|||Layered metasandstone or psammite, sandy or tuffaceous argillite with minor calc-silicate and albitic rocks; locally contains conglomerate, tuffaceous siltstone and fine-grained sandstone.|
39172|Aagot Member|65376|5|Briefly described|p110.|||||Unit in Wandearah Formation.||Interfingers with and intrudes Wardang Volcanics Member.|Conglomerates and coarse-grained metasedimentary rocks.|
39172|Aagot Member|70382|5|Briefly described|p29 Fig 3|Paleoproterozoic|Paleoproterozoic|Yorke Peninsula region.|||||Layered metasandstone, sandy or tuffaceous argillite.|
35877|Abminga Subsuite|2993|6|Mentioned|p12|Paleoproterozoic|Paleoproterozoic||1718 Ma|Basso Suite||||
35877|Abminga Subsuite|23347|2|Defined|p51 Tb. 1, p53, p55-56|Statherian|Statherian|Intrusive member of the Basso Suite (Willyama Supergroup).  Interlayered with Curnamona Gp. Age: ~1.71Ga; also 1699+/-10Ma, 1712+/-2Ma. Intrudes lower section of the Ethiudna Subgroup. Intercalated metavolcanics - detailed lithology included.|||||Red-brown weathering, light brown magnetite and pyrite-bearing, quartz-eye phyric, albitic, felsic metamorphosed rocks. Subvolcanic sills, pyroclastic flows & proximal volcaniclastics|13-SEP-12
35877|Abminga Subsuite|62993|6|Mentioned|p12|Paleoproterozoic|Paleoproterozoic||~1718 Ma|Basso Suite||||17-DEC-21
35877|Abminga Subsuite|63102|4|Described|p19,30,35,39-40,54|Statherian|Statherian|Geological province: Olary Domain, Curnamona Province. A-type igneous magmatism coeval with Curnamona Group sedimentation i.e. Montstephen Basalt. Cu mineralisation in Wiperaminga Subgroup in the Bimbowrie area is hosted psammopelitic sediments of the Peryhumuck Fomation interbedded with Abminga Subsuite volcanics.|1713+\-3 Ma|Unit of Basso Suite.||Intruded by Woman-in-White Amphibolite.|Metagranites (commonly as thick sills, and coarsely crystalline).|
35877|Abminga Subsuite|63866|5|Briefly described|p41|||Olary Domain, Curnamona Province.||Basso Suite||||
35877|Abminga Subsuite|64741|5|Briefly described|p305 Fig. 11|Paleoproterozoic|Paleoproterozoic|Of the Basso Suite. Age: ~1718Ma. Quartz-eye textured felsic metavolcanic rock.||||||07-FEB-11
35877|Abminga Subsuite|64944|6|Mentioned|p29 Tb. 1|Paleoproterozoic|Paleoproterozoic|Volcanic interbed within Tommie Wattie Formation. Geological province: Broken Hill Domain.||||||07-FEB-11
35877|Abminga Subsuite|66302|6|Mentioned|p36 Fig.9|Statherian|Statherian|Olary Domain, Curnamona Province. |ca. 1719-1715 Ma|Basso Suite||||
35877|Abminga Subsuite|69650|6|Mentioned|p16|||||||||
35877|Abminga Subsuite|70339|6|Mentioned|map legend|Paleoproterozoic|Paleoproterozoic|Curnamona Group includes volcanogenic metasediments related to Abminga Subsuite.||||||
35877|Abminga Subsuite|70340|6|Mentioned|map legend|Paleoproterozoic|Paleoproterozoic|Curnamona Group includes volcanogenic metasediments related to Abminga Subsuite.||||||
35877|Abminga Subsuite|70405|4|Described|p15, p33, p95|Paleoproterozoic|Paleoproterozoic|Also referred to as abmiga. Three samples described in detail.|1710 Ma - 1720 Ma|Basso Suite||Intrudes into Wiperaminga Subgroup|Volcaniclastic metasediments, metarhyolites with rounded quartz phenocrysts.Albitised metarhyolite flows are commonly massive but occasionally flow banded. Groundmass is commonly recrystallised to medium grain size with porphyritic texture .|
35877|Abminga Subsuite|70657|4|Described|p16, p25, p30-31, p45-47, p59|Statherian|Statherian|Curnamona Province. Also appears as the Abminga Suite. Extrusion and deposition was coeval with deposition of the Curnamona Group sediments. Has interbedded Cu-mineralised lenses. Alteration mentioned. U-Pb SHRIMP zircon ages range from ~1719 Ma to 1713 Ma. Appears as Abminga Volcanics on p47.|1702.5 +/- 7.6 Ma (Connor and Fanning, 2001).|Basso Suite.||Interbedded with Peryhumuck Formation. Is intruded by Woman-in-White Amphibolite.|Felsic volcanics and epiclastics, possible thin subvolcanic sills; generally mass-flow (proximal) volcaniclastics. A-type.|
35877|Abminga Subsuite|70658|5|Briefly described|p1-3, 5, 8, 10, 12, 21, 29, 32|Paleoproterozoic|Paleoproterozoic|Olary Domain, Curnamona Province. An age of ~1712 Ma is also given. Geochemistry briefly described.|~1718 Ma.|Basso Suite.||Intrudes Tommie Wattie Formation.|Voluminous A-type felsic volcanics, locally calc-silicate altered. Basal tuff unit.|
27099|Abrakurrie Limestone|22587|6|Mentioned|p79 Fig.7|Early Miocene|Late Oligocene|||||||
27099|Abrakurrie Limestone|22626|2|Defined|437,439,441-443,447|Early Miocene|Late Oligocene|Geol province Eucla Basin. Max thickness 100-120 m||||||
27099|Abrakurrie Limestone|22814|6|Mentioned|p258|Tertiary|Tertiary|||||||
27099|Abrakurrie Limestone|23768|5|Briefly described|p28 Fig.5, p31, p41|Middle Miocene|Early Miocene|Overlies Wilson Bluff Formation, underlies Nullarbor Limestone. Maximum thickness: >30m.  See also p113.||||||10-MAR-05
27099|Abrakurrie Limestone|24057|5|Briefly described|p97|Early Miocene|Early Oligocene|Geological Basin: Eucla Basin.||||||
27099|Abrakurrie Limestone|24094|4|Described|p273|Early Miocene|Late Oligocene|Disconformbly overlies the Wilson Bluff Limestone and the Toolinna Limestone. Overlain by Nullabor Limestone. Geological Province: Eucla Basin||||||16-MAR-05
27099|Abrakurrie Limestone|24347|5|Briefly described|p114|Early Miocene|Late Oligocene|Geological Province: Eucla Basin.||||||
27099|Abrakurrie Limestone|29856|6|Mentioned|p37|||||||||
27099|Abrakurrie Limestone|30268|6|Mentioned|p43|||||||||
27099|Abrakurrie Limestone|30976|6|Mentioned|Map legend|early Miocene|early Miocene|||||||
27099|Abrakurrie Limestone|31562|5|Briefly described|p13|||Early Miocene||||||
27099|Abrakurrie Limestone|31850|4|Described|p34|||Definition summary||||||
27099|Abrakurrie Limestone|31902|4|Described|Table 1|||Lower Miocene. Fig.1||||||11-JUL-13
27099|Abrakurrie Limestone|31903|6|Mentioned|Map legend|early Miocene|early Miocene|||||||
27099|Abrakurrie Limestone|31907|4|Described|p8|||See also Table, Fig.1||||||
27099|Abrakurrie Limestone|31908|4|Described|Table 1|||L.Miocene||||||
27099|Abrakurrie Limestone|31909|3|Fully described|p8|||L.Miocene?||||||
27099|Abrakurrie Limestone|32552|2|Defined|p192|early Miocene|early Miocene|See also p193-199.||||||27-AUG-18
27099|Abrakurrie Limestone|32648|6|Mentioned|p32|||Tertiary||||||
27099|Abrakurrie Limestone|32750|4|Described|p305|||||||||
27099|Abrakurrie Limestone|32752|6|Mentioned|p337|||||||||
27099|Abrakurrie Limestone|34192|6|Mentioned|Map legend|early Miocene|early Miocene|||||||
27099|Abrakurrie Limestone|34194|6|Mentioned|Map legend|early Miocene|early Miocene|||||||
27099|Abrakurrie Limestone|34232|6|Mentioned|p76|||Cavities.||||||
27099|Abrakurrie Limestone|35059|6|Mentioned|Table.19|||||||||
27099|Abrakurrie Limestone|35097|6|Mentioned|p17|||||||||
27099|Abrakurrie Limestone|35772|6|Mentioned|p11|||||||||
27099|Abrakurrie Limestone|36200|6|Mentioned|p15|||||||||
27099|Abrakurrie Limestone|36257|6|Mentioned|Table 2.1|||||||||
27099|Abrakurrie Limestone|36890|3|Fully described|p415|||||||||
27099|Abrakurrie Limestone|37577|6|Mentioned|p75|||||||||
27099|Abrakurrie Limestone|38553|6|Mentioned|p43|||||||||
27099|Abrakurrie Limestone|38602|6|Mentioned|p2|||||||||
27099|Abrakurrie Limestone|40410|6|Mentioned|p3|||||||||
27099|Abrakurrie Limestone|40992|6|Mentioned|Fig.23|||||||||
27099|Abrakurrie Limestone|41043|6|Mentioned|p87|||||||||
27099|Abrakurrie Limestone|41075|6|Mentioned|p18|||||||||
27099|Abrakurrie Limestone|41076|6|Mentioned|p70|||||||||
27099|Abrakurrie Limestone|41505|6|Mentioned|p6|||||||||
27099|Abrakurrie Limestone|41519|6|Mentioned|p169|||||||||
27099|Abrakurrie Limestone|42335|4|Described|p325|early Miocene|late Oligocene|Also further description p327-339.||||||27-AUG-18
27099|Abrakurrie Limestone|42734|5|Briefly described|map legend|Tertiary||||||||
27099|Abrakurrie Limestone|43026|5|Briefly described|Table 4,p590|||||||||
27099|Abrakurrie Limestone|43040|5|Briefly described|p861|||||||||
27099|Abrakurrie Limestone|43203|5|Briefly described|Map Legend||Miocene|Eucla Basin||||||
27099|Abrakurrie Limestone|43498|5|Briefly described|8||Early Miocene|||||||
27099|Abrakurrie Limestone|43667|6|Mentioned|Fig.3,p12|Early Miocene|Late Oligocene|||||||
27099|Abrakurrie Limestone|43702|6|Mentioned|p405|Miocene|Oligocene|||||||
27099|Abrakurrie Limestone|43713|6|Mentioned|p2|||||||||
27099|Abrakurrie Limestone|44133|5|Briefly described|p183, 180 Fig. 10.22|Early Miocene|Late Oligocene|Geological Province: Eucla Basin. Overlies: Wilson Bluff Limestone. Thickness: 100m. ||||||
27099|Abrakurrie Limestone|44145|4|Described|p550, p556-7, p555 fig 4-194, p561|Early Miocene|Early Miocene|Eucla Basin south of railway.  Max thickness > 91m. Age from echinoid and foraminifera fauna. Type section: west wall of Abrakurrie Cave.||||Disconformably overlies Wilson Bluff Limestone. Disconformably overlain by Nullarbor Limestone.|Yellowish porous bryozoan calcarenite and granule calcirudite. Mostly grainstone with some packstone.|08-OCT-15
27099|Abrakurrie Limestone|44412|14|Not recorded|map legend||Early Miocene|L.Miocene.||||||
27099|Abrakurrie Limestone|45149|6|Mentioned|p62|||||||||
27099|Abrakurrie Limestone|45168|6|Mentioned|p6, Table 1|||||||||
27099|Abrakurrie Limestone|61155|6|Mentioned|p4|Late Oligocene|Late Oligocene|Geological Province: Eucla Basin.||||||
27099|Abrakurrie Limestone|61197|6|Mentioned|p489|Early Miocene|Late Oligocene|Eucla Basin.||||||
27099|Abrakurrie Limestone|61517|5|Briefly described|p309|Miocene|Oligocene|Unconformably overlain by Roe Calcarenite.||||||
27099|Abrakurrie Limestone|62369|5|Briefly described|p409, p410 Fig.4|Early Miocene|Oligocene|Coarse-grained bryozoan calcarenite, distinctly cyclic, and contains numerous hardgrounds; locally dolomitised. Overlain by the Nullarbor limestone. Geological Province: Eucla Basin.||||||
27099|Abrakurrie Limestone|62640|5|Briefly described|p68, pp70-77.      |Early Miocene|Late Oligocene|Up to 100m thick. High porosity and permeability. |c.26 - c.24 Ma.|||Overlies Wilson Bluff Limestone. Is overlain by Nullarbor Limestone.|Metre-scale subtidal cycles capped by thin marine hardgrounds, forming well-lithified layers in otherwise friable carbonate.|
27099|Abrakurrie Limestone|64646|6|Mentioned|p23 Fig. 3, p24 Fig. 4|Early Miocene|Late Oligocene|Geological Province: Eucla Basin.||||||08-FEB-10
27099|Abrakurrie Limestone|65942|2|Defined|p76||Miocene|1967 Annual Report. ||Of Eucla Group.||||
27099|Abrakurrie Limestone|66131|6|Mentioned|p242 Fig.2|Miocene|Oligocene|Late Oligocene to Early Miocene in age (from p.242 Fig.2 - stratigraphic correlation chart).||||||
27099|Abrakurrie Limestone|67462|5|Briefly described|Map legend.|Miocene|Oligocene|Bunda Plateau, Eucla Basin.||||||
27099|Abrakurrie Limestone|67789|5|Briefly described|p34-35, 39-40, 45-46|Miocene|Oligocene|Eucla Basin. Up to 100m thick.||Eucla Group.||Overlies Wilson Bluff Limestone. Is overlain by Nullarbor Limestone.|A grainy neritic, bryozoan-rich, cool-water carbonate; contains numerous hard-grounds.|
27099|Abrakurrie Limestone|68715|6|Mentioned|p30 Fig.5|Aquitanian|Chattian|Bunda Plateau, Eucla Basin. ||||||
27099|Abrakurrie Limestone|69386|5|Briefly described|p7|Miocene|Oligocene|Eucla Basin.||||Overlies Wilson's Bluff Limestone.|Cool-water carbonate.|
27099|Abrakurrie Limestone|69598|5|Briefly described|p2, p9, p10, p11 Tb.1, p29 Tb.4|Early Miocene|Late Oligocene|Eucla Basin. Up to 120m thick. Potential carbon dioxide storage reservoir.||||Overlain by the Nullarbor Limestone.|Locally dolomitised coarse-grained bryozoan calcarenites and calcirudites.|
27099|Abrakurrie Limestone|69632|6|Mentioned|p26|Miocene|Oligocene|||Eucla Group|||Cool-water carbonate.|09-OCT-18
27099|Abrakurrie Limestone|69648|6|Mentioned|p25|||Deposited in cool to temperate waters on a platform that was drowned for part of the time, in central and southern parts of Eucla Basin (Lowry 1970; James and Bone, 1991). Age: Oligocene?||||||
27099|Abrakurrie Limestone|70397|5|Briefly described|p1-3|Early Miocene|Late Oligocene|Eucla Basin. Depositional environment: cool-temperate, open-marine shelf.||Unit of Eucla Group.||Unconformably overlain by Nullabor Limestone. Unconformably underlain by Wilson Bluff Limestone.|Medium- to coarse-grained bryozoan facies.|29-JUL-19
27099|Abrakurrie Limestone|70771|4|Described|p3-p4, p7-p8, p11-p12|Early Miocene|Late Oligocene|Eucla Platform, Eucla Basin. Seperated into two informal units (discussed p3). This unit is fossiliferous and contains abundant bryozoans, foraminifera, bivalves, brachiopods and echinoids; serpulid worms, solitary corals, gastropods and coralline algae also occur. This unit has a maximum thickness of up to 90m; however, a greater original thickness to the south has been suggested (Lowry, 1967). Interpreted to have been deposited on a shallow, open shelf with water depths up to 100m.   [The author assigns this unit to the Eucla Group however this term is obsolete]. See also p27, p31, p53-p58, p60-p61.||Eucla Group||Disconformably overlies the Wilson Bluff Limestone. Disconformably overlain by the Nullarbor Limestone and the Roe Calcarenite.|Moderately well-sorted, thin-bedded, friable fossiliferous calcarenite and indurated and thick-bedded calc-arenite.|
27099|Abrakurrie Limestone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||calcirudite, calcarenite|
27099|Abrakurrie Limestone|71361|4|Described|p5, p15, p17, p23|Early Miocene|Late Oligocene|Eucla Basin.  [NB The author assigns this formation to the disused Eucla Group on the basis of references to older literature - Lowry 1970]. Interpreted to have been deposited in a cool water, neritic envrionment. See also  p119, p140, p144, p192-p195.||Eucla Group||Unconformably overlies the Wilson Bluff Limestone. Unconformably overlain by the Nullarbor Limestone.|Medium to coarse grained, bryozoan grainstone to packstone with local fine-gained wackestone and coarse-grained floatstone and rudstone.|
27099|Abrakurrie Limestone|71618|6|Mentioned|p124|Cenozoic|Cenozoic|Geological province: Eucla Basin.||Unit of Eucla Group.||||05-SEP-19
27099|Abrakurrie Limestone|71891|5|Briefly described|p7|Cenozoic|Cenozoic|Eucla Basin. Thin (generally <10m thick) unit that is interpreted to have been deposited on a partly to completely drowned platform.||||Overlain by the Nullarbor Limestone. Overlies the Wilsons Bluff Limestone.|Limestone.|
27099|Abrakurrie Limestone|72344|5|Briefly described|p5|||Eucla Basin. Generally less than 10m thick. Forms a distinct yellow-brown band in the Bunda Cliffs.||||Overlies the Wilson Bluff Limestone. Overlain by the Nullarbor Limestone.|Yellowish coarse-grained bryozoan calcarenite and calcirudite, distinctly cyclic and contains numerous hardgrounds; locally dolomitized.|
27099|Abrakurrie Limestone|72465|5|Briefly described|p9|Tertiary|Tertiary|Eucla Basin, Coompana Province. Generally thin (<10m thick) unit. Forms a distinctive yellow-brown band in the Bunda Cliffs. Partly to completely drowned platform deposits.||||Overlies Wilson Bluff Limestone. Is overlain by Nullarbor Limestone.|Yellowish coarse-grained bryozoan calcarenite and calcirudite, distinctly cyclic, and contains numerous hardgrounds; locally dolomitized.|
27099|Abrakurrie Limestone|72466|5|Briefly described|p9|Tertiary|Tertiary|Benbow et al. (1995). Eucla Basin, Coompana Province. Generally thin (<10m thick). Deposited on a partly to completely drowned platform. Forms a distinct yellow-brown band in the Bunda Cliffs.||||Overlies Wilson Bluff Limestone. Is overlain by Nullarbor Limestone.|Yellowish coarse-grained bryozoan calcarenite and calcirudite, distinctly cyclic, and contains numerous hardgrounds; locally dolomitized.|
27099|Abrakurrie Limestone|72467|5|Briefly described|p9|Tertiary|Tertiary|Eucla Basin, Coompana Province. Generally thin (<10m thick) unit. Forms a distinctive yellow-brown band in the Bunda Cliffs. Partly to completely drowned platform deposits.||||Overlies Wilson Bluff Limestone. Is overlain by Nullarbor Limestone.|Yellowish coarse-grained bryozoan calcarenite and calcirudite, distinctly cyclic, and contains numerous hardgrounds; locally dolomitized.|
27099|Abrakurrie Limestone|72468|5|Briefly described|p9|||Eucla Basin. Thin; generally less than 10 m thick. Deposited on a partly to completely drowned platform. Forms a distinct yellow-brown band in the Bunda Cliffs.||||Underlain by Wilson Bluff Limestone. Overlain by Nullarbor Limestone.|Yellowish coarse-grained bryozoan calcarenite and calcirudite, distinctly cyclic, and contains numerous hardgrounds; locally dolomitized.|
27099|Abrakurrie Limestone|72469|5|Briefly described|p9|||Eucla Basin. Thin; generally less than 10 m thick. Deposited on a partly to completely drowned platform. Forms a distinct yellow-brown band in the Bunda Cliffs.||||Underlain by Wilson Bluff Limestone. Overlain by Nullarbor Limestone.|Yellowish coarse-grained bryozoan calcarenite and calcirudite, distinctly cyclic, and contains numerous hardgrounds; locally dolomitized.|
27099|Abrakurrie Limestone|72470|5|Briefly described|p9|||Eucla Basin. Thin; generally less than 10 m thick. Deposited on a partly to completely drowned platform. Forms a distinct yellow-brown band in the Bunda Cliffs.||||Underlain by Wilson Bluff Limestone. Overlain by Nullarbor Limestone.|Yellowish coarse-grained bryozoan calcarenite and calcirudite, distinctly cyclic, and contains numerous hardgrounds; locally dolomitized.|
27099|Abrakurrie Limestone|72471|5|Briefly described|p9|||Eucla Basin. Thin; generally less than 10 m thick. Deposited on a partly to completely drowned platform. Forms a distinct yellow-brown band in the Bunda Cliffs.||||Underlain by Wilson Bluff Limestone. Overlain by Nullarbor Limestone.|Yellowish coarse-grained bryozoan calcarenite and calcirudite, distinctly cyclic, and contains numerous hardgrounds; locally dolomitized.|
27099|Abrakurrie Limestone|72472|5|Briefly described|p9|||Eucla Basin. Thin; generally less than 10 m thick. Deposited on a partly to completely drowned platform. Forms a distinct yellow-brown band in the Bunda Cliffs.||||Underlain by Wilson Bluff Limestone. Overlain by Nullarbor Limestone.|Yellowish coarse-grained bryozoan calcarenite and calcirudite, distinctly cyclic, and contains numerous hardgrounds; locally dolomitized.|
27099|Abrakurrie Limestone|73084|6|Mentioned|p16|Miocene|Oligocene|||||||
27099|Abrakurrie Limestone|73641|5|Briefly described|p5|Miocene|Oligocene|Eucla Basin. <10m thick. Drowned platform environment.||||Overlies Wilson Bluff Limestone. Is overlain by Nullarbor Limestone.|Yellowish coarse-grained bryozoan calcarenite and calcirudite, containing numerous hardgrounds; locally dolomitized.|
75964|Acraman impact ejecta layer|63811|6|Mentioned|p499, Fig 2|Ediacaran|Ediacaran|Regional stratigraphic marker.  Less diversification in marine single cell biota below this layer. Occurs within Dey Dey Mudstone in Giles 1, Officer Basin.||||||
75964|Acraman impact ejecta layer|67912|6|Mentioned|p13-14|Ediacaran|Ediacaran|A widespread, precise marker bed.|580-570 Ma.||||A 7mm thick sand layer with a thin shale lamina, surrounded by a green shale envelope 20mm thick.|
75964|Acraman impact ejecta layer|72451|4|Described|p4, p5|Late Proterozoic|Late Proterozoic|Type section [said to be] in Brachina and Bunyeroo Gorges. Acronym AEIL or AIEL [both used]. Forms a distinct horizon (< 6cm thick) with a characteristic stratigraphic succession. |c. 580 Ma|||Found within Bunyeroo Formation and other time-equivalent units across the Flinders Ranges, Stuart Shelf, Officer Basin and Amadeus Basin.|Basal layer of volcanic rock fragments in a sandy matrix forms a sharp contact with the underlying mudstone. Basal layer overlain by a thin sandy mudstone layer. A rare cross bedded sandstone occurs at the termination of the AEIL in Brachina Gorge.|
80750|Adder Dolerite|71862|6|Mentioned|p8 Fig.3|||Archean? Asociated with Cooyerdoo Granite?||||||28-FEB-19
82822|Albala-Karoo Syenogranite|72947|2|Defined|p7, p9, p15-17, p21|Stenian|Stenian|Coompana Province, eastern. Named after Albala-Karoo Rockhole. Type locality: CDP003 (drillhole 299057, interval 265.00-267.80 m). Represent high-grade metamorphism, anatexis, deformation and magmatism. Contains rare feldspar phenocrysts that are similar to those in the host, which suggests the syenogranite magma intruded an incompletely crystallised body enabling individual grains to be plucked out of the host. Forms sheets within the plutons of the Koonalda Suite and thus has the same distribution, which are mostly concentrated within a northeast-trending corridor between the Palinar and Border shear zones. The sheets have boundaries that range from sharp and straight, to sharp and irregular with the contact following the grain boundaries in the host granites, to gradational. Sheets have a maximum thickness of 4 m.|1150.48 +/- 0.52 Ma CA TIMS|Koonalda Suite, Moodini Supersuite||Contemporaneous with and intrudes Koonalda Suite.|Pink to brown, massive, fine- to medium-grained and equigranular to locally porphyritic syenogranite.|
80536|Albala-karoo Syenogranite|72242|5|Briefly described|p30|Stenian|Stenian|Associated with Maralinga Event (including Musgrave Orogeny). Coeval with Moodini Supersuite and Maerdayerrah Shoshonite. Intersected in CDP003 and CDP 005 drillholes, forming late cross-cutting intrusions.|||||Equigranular biotite micro-syeno- to monzogranitic syenogranite.|
68089|Alconie Formation|60485|6|Mentioned|p29|||Graphitic pelite rocks.||||||03-MAR-05
68089|Alconie Formation|61736|5|Briefly described|p666 Fig. 3|Paleoproterozoic|Paleoproterozoic|Of Mount Howden Subgroup (Strathearn Group). Geological province: Olary Domain.||||||
68089|Alconie Formation|62535|5|Briefly described|p666 Fig.3, p672|Paleoproterozoic|Paleoproterozoic|Olary Domain.||Mount Howden Subgroup.||||
68089|Alconie Formation|62993|6|Mentioned|p3, p37|Paleoproterozoic|Paleoproterozoic|Olary Domain.||Mount Howden Subgroup||Overlies Plumbago Formation. Overlain by Mooleulooloo Formation||19-DEC-21
68089|Alconie Formation|63102|4|Described|p14,32-37|||Geological province: Olary Domain, Curnamona Province. Formerly known as Alconie Pelite (Conor, 2000a). Underlain by a sequence of thin graphitic pelite, which is equivalent to Plumbago Formation. Significant thickness variations observed on opposite limbs of Mount Howden Syncline (see p35 for possible reasons). Change in Nd isotope signature (Barovich 2003) indicate a switch in sediment provenance away from possible central Australian source.||Unit of Mount Howden Subgroup.||Equivalent to Cartwights Creek Metasediments.|Lower aluminous pelite unit; andalusite-rich with large chiastolite porphyroblasts, and an upper dark grey, fine-grained, graphitic psammopelite.|22-OCT-19
68089|Alconie Formation|64741|4|Described|p301 Fig. 4, p311|Paleoproterozoic|Paleoproterozoic|Of Mount Howden Subgroup (Strathearn Group). Geol.prov: Olary Domain. Thickly interlayered graphitic metasiltstone and aluminous pelite grading upwards into Looleulooloo Formation. Equivalent of Cartwrights Creek Metasediments in Broken Hill Domain.||||||07-FEB-11
68089|Alconie Formation|64742|6|Mentioned|p321 Fig.3, p323.|||||Unit in Mount Howden Subgroup.|||Psammite, psammopelite, pelite, calc-albite metasediments, chiastolite schist, andalusite schist.|05-MAR-13
68089|Alconie Formation|64944|5|Briefly described|p28 Fig. 1, p29 Tb. 1|Paleoproterozoic|Paleoproterozoic|Of Strathearn Group. Geological province: Olary Domain. Graphitic chiastolite pelite and metasiltstone. Equivalent to Cartwrights Creek Metasediments in Broken Hill Domain.||||||07-FEB-11
68089|Alconie Formation|66302|4|Described|p36 Fig.9, p38, p39|Statherian|Statherian|Olary Domain, Curnamona Province.||Mount Howden Subgroup||Overlain by the Mooleulooloo Formation.|Thickly layered graphitic metasiltstone, sandstone and andalusite mudstone.|
68089|Alconie Formation|70405|5|Briefly described|p9 table 1, p30, p43 Table 3|Paleoproterozoic|Paleoproterozoic|A local fine grained calc-silicate lens is reminiscent of King Gunnia Calc-silicate Member in the broken hill domain.|1640 Ma - 1655 Ma|Mount Howden Subgroup||Correlates with Carwrights Creek Metasediments.|Pelite dominated with relatively coarse grained pelitic schists contain chiastolite porphyroblasts and thin, fine-medium grained psammite interbeds. Psammite beds are graded with reversal of grain size variation.|
68089|Alconie Formation|70657|4|Described|p14-15, p17, p24, p33-34, p40-44|Statherian|Statherian|Curnamona Province, Olary Domain. Formerly the Alconie Pelite (Conor, 2007). Famous for large chiastolite porphyroblasts (the red variety is called howdenite).|<1693 Ma - >1655 Ma|Basal Mount Howden Subgroup||Underlies Mooleulooloo Formation. Overlies Plumbago Formation gradationally and ?Walparuta Formation (Saltbush Group). Equivalent to Cartwrights Creek Metasediments in Broken Hill Domain.|Thickly interlayered graphitic metasiltstone, psammite and andalusite pelite with chiastolite-bearing pelite at the base. Distinctly graphitic base.|
68089|Alconie Formation|70658|5|Briefly described|p7, 15|Paleoproterozoic|Paleoproterozoic|Olary Domain, Curnamona Province.||Mount Howden Subgroup.||Locally overlies Plumbago Formation. Equivalent to Cartwrights Creek Metasediments.||
68089|Alconie Formation|70829|6|Mentioned|p33|||Curnamona Province. Known to contain graphite which may contribute to the high conductivity of Olary Domain lithosphere.||||||
39599|Alcurra Dolerite|60679|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Dolerite dykes. Geological Province: Musgrave Block.||||||
39599|Alcurra Dolerite|61154|2|Defined|p42 App., p13, p15-16, p44|Mesoproterozoic|Mesoproterozoic|Dolerite with ophitic to subophitic texture contains plagioclase. Unconformable over Dean Quartzite. Intrudes Pitjantjatjara Supersuite (Kugera Gr. and Ayers Range Gr). Intruded by Angatja Granite. Age: 1080Ma. Geol.Prov: Musgrave Block.||||||01-SEP-09
39599|Alcurra Dolerite|61524|5|Briefly described|p16|||Mafic dykes associated with the Giles Complex. Geological Province: Musgrave Province.||||||
39599|Alcurra Dolerite|61733|5|Briefly described|p46, p56|||Musgrave Block. Has subduction-related isotopic and geochemical signatures. Emplaced during the Warakurna igneous event at c.1.08-1.05 Ga.|c.1.08 Ga.||||High-Mg, low-Ti tholeiites.|
39599|Alcurra Dolerite|64722|6|Mentioned|p17|Stenian|Stenian|Of a similar age to granites dated at 1080-1070 Ma.|||||Mafic tholeiitic dykes.|11-APR-12
39599|Alcurra Dolerite|64745|5|Briefly described|p376|Stenian|Stenian|Dykes. Age: ca. 1.08 Ga (Sm-Nd isochron Plag-Opx-Cpx. Zhao and McCulloch, 1993). May represent feeder system to Giles Intrusions. Geol. Prov: Musgrave Province.||||||
39599|Alcurra Dolerite|65135|6|Mentioned|p17|Stenian|Stenian|~1070 Ma. Shows geochemical similarities to Giles Event intrusives and the Warakurna Large Igneous Province.||||||
39599|Alcurra Dolerite|65369|5|Briefly described|p35|||Central Australian intraplate (flood-type) basalt.||||||19-MAR-12
39599|Alcurra Dolerite|65693|4|Described|p4,p7- p8 Fig.5, p9-12 Figs. 8-10.|||See also Alcurra Suite, Alcurra suite. Geochemistry is different from Tollu Group: detailed in text. Ages are Ar/Ar from Schmidt et al. (2006).|1085 +/- 2 to 1068 +/- 2 Ma|Unit in Alcurra Suite.|||Relatively evolved, Fe-rich, incompatible trace element-rich suite of tholeiitic intrusions.|22-APR-20
39599|Alcurra Dolerite|65833|5|Briefly described|p17|Stenian|Stenian|Formed during ~1075 Ma Giles Event. Intrudes Pitjantjatjara Supersuite.||||||
39599|Alcurra Dolerite|65906|6|Mentioned|p7|Mesoproterozoic|Mesoproterozoic|~1070 Ma.||||||
39599|Alcurra Dolerite|67128|6|Mentioned|p6|||||Warakurna Supersuite.|||Mafic dykes.|
39599|Alcurra Dolerite|67244|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic||c.1067 Ma.|Unit in Warakurna Supersuite.|||Dykes, sills or plugs mainly of dolerite; also of olivine gabbro, accessory biotite, massive to weakly flow-banded; and fine- to medium-grained plagioclase-phyric gabbro, ophitic texture, plagioclase phenocrysts and glomerophenocrysts to 2 cm.|11-APR-12
39599|Alcurra Dolerite|67372|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic||c.1068 Ma.|Unit in Warakurna Supersuite.|||Dykes, sills or plugs mainly of dolerite and metadolerite but also of olivine gabbro, olivine norite, ferronorite, and ferrodiorite.|
39599|Alcurra Dolerite|67375|4|Described|p13, p19 Fig.11, pp36-37, p41, pp332-339|Mesoproterozoic|Mesoproterozoic|A suite of rocks including the Alcurra Dolerite dyke swarm, small intrusions emplaced peripheral to the Warakurna Supersuite, and the compositionally equivalent olivine-rich gabbros, olivine norites, ferronorites and ferrodiorites which host the Nebo-Babel nickel-copper-PGE sulfide mineralization.|1068 +/- 7 - 1067 +/- 8 Ma (Kirkland et al. 2009).|Unit in Warakurna Supersuite.||Intrudes the Smoke Hill Volcanics and Giles Suite.|Dykes, sills and plugs mainly of dolerite but also of olivine gabbros, olivine norites, ferronorites and ferrodiorites.|
39599|Alcurra Dolerite|67553|5|Briefly described|p11,20,34,37-41,p65, 89,95|Stenian|Stenian|Geological province: Musgrave Province, North Australian Craton. Makes up the Warakurna Supersuite component within the Walpa Pulka Zone. Intrusive age from GSWA 194354, coeval with emplacement of Smoke Hill Volcanics. Highly evolved iron-rich tholeiitic intrusions intruding at a relatively late stage in the Giles Event at c. 1067 Ma. At least locally, these rocks are directly related to orthomagmatic nickel-copper mineralization (Howard et al., 2009).|1068+\-7 Ma|Unit of Warakurna Supersuite.||||06-AUG-19
39599|Alcurra Dolerite|68995|6|Mentioned|p1, p8, p50-56, p61, p64-65.|Mesoproterozoic|Mesoproterozoic|Referred to on p1 as the informal Alcurra Dolerite dyke swarm. Intruded during the Mesoproterozoic Giles Event. Source and origin of this unit is discussed in great detail.||||||
39599|Alcurra Dolerite|68996|5|Briefly described|p7, 24-25, 28-29, 32,33, 35-46,53,54,66|Mesoproterozoic|Mesoproterozoic|Hosts significant mineralization of the Nebo-Babel Ni-Cu-PGE deposit. Includes Saturn gabbro. Age range from current dating may not recognise prolonged magmatism suggested from field relationships. See also Alcurra Dolerite Suite p9.|1072-1068 Ma magmatic||Includes Saturn gabbro.||Dolerite dykes and sills. Average density of 2.98+/-0.17g/cm^3|
39599|Alcurra Dolerite|69003|5|Briefly described|p50|Mesoproterozoic|Mesoproterozoic|Associated with the Giles Event. Hosts the orthomagmatic Ni-Cu-PGE mineralisation of the Nebo-Babel deposit, described in some detail on p51.|c.1070 Ma.||||Iron-rich tholeiitic mafic dykes and sills.|
39599|Alcurra Dolerite|69009|5|Briefly described|Map Legend|Stenian|Stenian||c. 1068 Ma|Of the Warakurna Supersuite.|||Comprises dykes, sills, or plugs, with olivine gabbro, olivine norite, ferronorite, and ferrodiorite.|
39599|Alcurra Dolerite|69091|4|Described|p54 Fig.4.2, p74, p103 Fig.5.6|Mesoproterozoic|Mesoproterozoic|Warakurna Large Igneous Province (Wingate et al., 2004). Hogarth Formation is compositionally identical with an identical crystallisation age of 1068 +/- 7 Ma. Appears as Alcurra Dolerite Suite on p132, p134 Fig.6.2, p137-138, p141 Fig.6.8, p144, p204-205.|1068 +/- 7 Ma|Warakurna Supersuite|Saturn gabbro||Mafic intrusions; most are relatively small dykes and sills, however some larger intrusions exist.|
39599|Alcurra Dolerite|69153|5|Briefly described|GEOL_LUT_CSV files;GEOCHRON/194354.1.pdf|Mesoproterozoic|Mesoproterozoic|Geochron analysis (194354) of medium- to coarse-grained, ophitic gabbro dyke. 20 analyses|1067+/-8 Ma SHRIMP-A|Warakurna Supersuite|||Dolerite in dykes, sills, or plugs, with olivine gabbro, olivine norite, mesocratic orthopyroxene(-olivine) ferronorite to ferrodiorite|
39599|Alcurra Dolerite|69427|6|Mentioned|p12:46|||Musgrave Province.||||Is correlated with Stuart Pass Dolerite (Aileron Province).||12-JUL-16
39599|Alcurra Dolerite|69428|6|Mentioned|p13:16|||Musgrave Province.||||Correlated with the Stuart Pass Dolerite.||12-JUL-16
39599|Alcurra Dolerite|69436|4|Described|p21:1, 4, 11-14, 20-21|Mesoproterozoic|Mesoproterozoic|Edgoose et al. (1993). Widespread throughout Musgrave Province. Related to the Giles Event (1085-1040 Ma). Chilled margins on some dykes suggest shallow-level intrusions. Similar geochemistry to Mount Harris Basalt suggests a common source. As potential feeders for the Giles Complex, some larger dykes have potential for Cu-Ni-Co mineralisation. Geochronology by Camacho et al. (1991) and Zhao and McCulloch (1993) respectively.|1054 +/- 14 Ma (Rb-Sr); 1090 +/- 32 Ma (Sm-Nd).|Warakurna Supersuite.||Intrudes Musgravian gneiss and Pitjantjatjara Supersuite. Is intruded by Angatja Suite.|Extensive intrusions of dolerite and subordinate gabbro dykes, typically 1-3m wide, but up to 8m wide and 6km long. Geochemically homogeneous olivine tholeiite, generally ophitic to sub-ophitic. Locally metamorphosed to garnet granulite facies.|12-JUL-16
39599|Alcurra Dolerite|69437|6|Mentioned|p22:11-12|||Associated with the c.1070 Ma Warakurna Large Igneous Province. Emplaced within the Musgrave Province.||||||12-JUL-16
39599|Alcurra Dolerite|69438|6|Mentioned|p23:9|||Intrudes basement rocks of the Aileron Province.||||||12-JUL-16
39599|Alcurra Dolerite|69640|6|Mentioned|p11|Proterozoic|Proterozoic|Musgrave Province.||||Intrudes the Pitjantjatjara Supersuite.||
39599|Alcurra Dolerite|69655|6|Mentioned|p58|||||||||
39599|Alcurra Dolerite|69729|5|Briefly described|p68, p74 Fig.8, p80-84, p86|Mesoproterozoic|Mesoproterozoic|Edgoose et al. (1993); Scrimgeour et al. (1999). Warakurna Large Igneous Province. Originally defined from the Kulgera region (NT). Geochemistry and provenance discussed; trace element plot.|c.1078 Ma to 1073 Ma.|||Is cross-cut by Kullal Dyle Suite.||
39599|Alcurra Dolerite|70083|6|Mentioned|p207|||Musgrave Inlier. Associated with the Giles Event.|~1085-1050 Ma.|Giles Complex.||Intrudes Birksgate Complex.||
39599|Alcurra Dolerite|70338|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic||||||Dolerite, dark grey, medium- to fine-grained, olivine, hypersthene. Poikilitic texture.|
39599|Alcurra Dolerite|70634|4|Described|100k_geologyp_lut,csv|Mesoproterozoic|Mesoproterozoic|SHRIMP age from dolerite (19454.1.pdf)|1067 Ma - 1068 Ma (Isotopic) 1067  (SHRIMP)|Warakurna Supersuite|||Dolerite dykes, sills or plugs with olivine gabbro, olivine norite, ferronorite and ferrodiorite. Fine-medium grained plagioclase-phyric dolerite and gabbro. Olivine rich gabbro, fine-grained, mesocratic ferronorite to ferrodiorite.|
39599|Alcurra Dolerite|70793|4|Described|GEOL_LUT_CSV files + geochron files|Mesoproterozoic|Mesoproterozoic|Geological province: Musgrave Province. Of Warakurna Large Igneous Province. Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma); Warakurna Supersuite Magmatic Event (1084-1040 Ma); Giles Event (1085-1040 Ma). Sample GSWA 194354 (gabbro dyke) yielded an interpreted (207Pb*/206Pb* and 238U/206Pb* concordia) magmatic crystallisation age of 1067+\-8 Ma. See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop14_lut.csv, 100k_interpgeol_lut.csv, 500k_interpgeop_lut.csv, 100k_geologyl_lut.csv, 250k_interpgeol_lut.csv, 500k_interpgeol_lut.csv, 2_5m_interpdykel15_lut.csv.|1068-1067 Ma (inferred)|Unit of Warakurna Supersuite.|||Dolerite in dykes, sills, or plugs, with olivine gabbro, olivine norite, ferronorite, and ferrodiorite; mesocratic pox-olivine ferronorite to ferrodiorite.|
39599|Alcurra Dolerite|70826|6|Mentioned|p10, p14 tbl 5|Mesoproterozoic|Mesoproterozoic|Musgrave Province. |1068-1067 Ma|Warakurna Supersuite.||||20-MAY-20
39599|Alcurra Dolerite|70831|5|Briefly described|p4-p5|Stenian|Stenian|Musgrave Province.|c. 1085-1040 Ma|Warakurna Supersuite||||
39599|Alcurra Dolerite|71170|5|Briefly described|p6|||||||||
39599|Alcurra Dolerite|71210|5|Briefly described|p5, p10-p12, p15, p20, p43,|Stenian|Stenian|Musgrave Province. C. 1080 Ma age is derived from Edgoose et al., 1993; Scrimgeour et al., 1999 and Howard et al., 2009c. Hosts most of the magmatic sulphide mineralisation of the Musgrave Province, including the Nebo-Babel Ni-Cu-PGE deposit. Previously referred to as the G3 member of the Giles Suite. See also p46, p50, p66-p67, p69, p76, p109, p114, p134, p139.|c. 1080 Ma -1068 Ma||||Dolerite, olivine gabbros, norites, ferronorites and diorites.|
39599|Alcurra Dolerite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||dolerite|
39599|Alcurra Dolerite|71268|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Of Warakurna Large Igneous Province. Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma); Warakurna Supersuite Magmatic Event (1084-1040 Ma); Giles Event (1085-1040 Ma). Sample GSWA 194354 (gabbro dyke) yielded a weight mean 207Pb/206Pb age of 1067+\-8 Ma, interpreted as magmatic crystallisation age. See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeop16_lut.csv, 100k_interpgeol_lut.csv, 100k_geologyl_lut.csv, 250k_interpgeol_lut.csv, 500k_interpgeol_lut.csv, 2_5m_interpdykel15_lut.csv.|1068+\-4 Ma; 1067+\-8 Ma|Unit of Warakurna Supersuite.|||Dolerite dykes and plugs; plagioclase-phyric dolerite and gabbro; ferronorite: mesocratic opx-olivine, magnetite-rich; mesocratic opx ferrnonorite to ferrodiorite.|
39599|Alcurra Dolerite|71321|6|Mentioned|p1,11,23, 50,58,64|Stenian|Stenian|Geological province: Musgrave Province. Comprises part of basement to the Musgrave Province i.e. intrudes and cross-cuts Musgravian-aged gneisses and granites. Associated with c. 1080 Ma Giles Event (p11 for references).||||||24-OCT-19
39599|Alcurra Dolerite|71416|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Warakurna Large Igneous Province. Interpreted age from correlation with Giles Complex.|~1080 Ma.|Warakurna Supersuite.||Correlated with Giles Supersuite.|Massive olivine dolerite, mainly E-trending dykes.|
39599|Alcurra Dolerite|71592|5|Briefly described|Appendix A.|||Musgrave Province.|1067+/-8 Ma (crystallisation: U-Pb zircon SHRIMP)||||Gabbro with ophitic texture and interstitial pyroxene.|
39599|Alcurra Dolerite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoproterozoic|Mesoproterozoic||Max age 1068+/-4, min 1067+/-8 Ma.|Warakurna Supersuite|||Dolerite in dykes, sills, or plugs, with olivine gabbro, olivine norite, ferronorite, and ferrodiorite.|
39599|Alcurra Dolerite|72094|6|Mentioned|p2, p3 Fig 2|Mesoproterozoic|Mesoproterozoic|Musgrave Province.||Unit of Warakurna Supersuite.||||
39599|Alcurra Dolerite|72238|5|Briefly described|p34-36,38-42|Stenian|Stenian|Geological province: Musgrave Province. Dimensions: mainly <10m, rarely up to 80m wide. Associated with coeval Giles Complex mafic-ultramafic intrusions (prospective for orthomagmatic Ni-Cu PGE mineralisation (Howard et al. 2009). Forms part of the Warakurna Large Igneous Province (Wingate, Pirajno and Morris 2004). Generally of lower olivine content than Amata Dolerite. Locally crosscut by Amata Dolerite dykes. Commonly shows evidence for contamination by host rocks. Sm-Nd isochron age: 1110+\-56 Ma.|c. 1080 Ma|||||
39599|Alcurra Dolerite|72443|5|Briefly described|p737, 739, p748, p751-752, p757|||Emplaced over much of central and western Australia and represents much of the Warakurna Large Igneous Province.|1078-1073 Ma|Warakurna Supersuite|||Dolerite dykes and sills.|
39599|Alcurra Dolerite|72476|6|Mentioned|p35, 39|||Musgrave Province. Intrusion of these sills and dykes is suggested to have reset the apatite U-Pb clock in the easternmost parts of the Province. Associated with the mafic/ultramafic Warakurna Large Igneous Province. See also reference to Alcurra Dolerites (p25).||||||
39599|Alcurra Dolerite|73232|6|Mentioned|p5|||Musgrave Province. [Emplaced] during the Giles Event. Includes dykes.||Giles Complex||Intrudes Birksgate Complex and Pitjantjatjara Supersuite.||
39599|Alcurra Dolerite|73437|6|Mentioned|p151|Mesoproterozoic|Mesoproterozoic|||Warakurna Supersuite||||
27074|Aldinga Member|22525|6|Mentioned|p37||Eocene|superseded by Port Willunga Formation||||||
27074|Aldinga Member|22528|6|Mentioned|p43 Fig2||Oligocene|||||||
27074|Aldinga Member|22541|4|Described|p 29, Fig 1, 3||Late Eocene|Port Willunga Formation.||||||12-NOV-08
27074|Aldinga Member|22587|6|Mentioned|p79 Fig.7|Late Eocene|Late Eocene|||||||
27074|Aldinga Member|30250|1|Redefined|p2|late Eocene|late Eocene|||||||
27074|Aldinga Member|35542|6|Mentioned|p2|||||||||
27074|Aldinga Member|35689|1|Redefined|p22|late Eocene|late Eocene|||||||
27074|Aldinga Member|36127|5|Briefly described|p11|||See also p7.||||||18-SEP-18
27074|Aldinga Member|36244|6|Mentioned|p2|||Redefined by Cooper 1977, 1979.||||||
27074|Aldinga Member|36500|6|Mentioned|Fig.4|||||||||
27074|Aldinga Member|37324|6|Mentioned|p11|||||||||
27074|Aldinga Member|37852|6|Mentioned|p2|||||||||
27074|Aldinga Member|38107|4|Described|p36|||||||||
27074|Aldinga Member|39351|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
27074|Aldinga Member|40238|6|Mentioned|p324|||||||||
27074|Aldinga Member|40429|6|Mentioned|p28|||||||||
27074|Aldinga Member|40453|5|Briefly described|p57|||||||||
27074|Aldinga Member|40877|5|Briefly described|p50|||||||||
27074|Aldinga Member|40969|6|Mentioned|p10|||||||||
27074|Aldinga Member|40970|6|Mentioned|p16|||||||||
27074|Aldinga Member|41025|5|Briefly described|p167|||||||||
27074|Aldinga Member|41495|6|Mentioned|Table 5|||||||||
27074|Aldinga Member|41513|6|Mentioned|p43|||||||||
27074|Aldinga Member|41517|6|Mentioned|p137|||See also Fig.5||||||
27074|Aldinga Member|41520|5|Briefly described|Fig.5|||||||||
27074|Aldinga Member|41626|6|Mentioned|p54|||||||||
27074|Aldinga Member|42574|6|Mentioned|Fig.2 P242|||||||||
27074|Aldinga Member|44133|5|Briefly described|p165 Fig. 10.11, 168|Early Oligocene|Early Oligocene|Geological Province: Saint Vincent Basin. Of the Port Willunga Formation.||||||
27074|Aldinga Member|60538|5|Briefly described|p479 Fig. 18|Oligocene|Eocene|Geological Province: Saint Vincent Basin. Of the Port Willunga Formation.||||||
27074|Aldinga Member|61155|5|Briefly described|p3, p17|Early Oligocene|Late Eocene|Of the Port Willunga Formation. Overlies the Chinaman Gully Formation. Age: 37-36Ma. Geological Province: St Vincent Basin.||||||
27074|Aldinga Member|64397|5|Briefly described|p232 Fig. 1A, p233|Miocene|Oligocene|Lower part of Port Willunga Formation. Heterolithic sand, sandtsone, mudstone and marl. Detailed lithological chart presented - p237, Fig. 5. See also p245 Fig. 11. Geological province: St Vincent Basin.||||||
27074|Aldinga Member|64993|5|Briefly described|p2p Fig. 5|||Of Port Willunga Formation. Geological province: St Vincent Basin. Calcarenite, bryozoal calcarenite and bryozoal marl.||||||30-MAR-09
27074|Aldinga Member|65375|4|Described|pp35-36, p38|Oligocene|Oligocene|c.6m thick.||Lower unit in Port Willunga Formation.||Overlies and grades into Rogue Formation. Is overlain by Ruwarang Member.|Sandy, skeletal limestone and calcareous sandstone; lenses of thin silty limestone, siltstone and glauconitic sandy layers.|18-SEP-18
27074|Aldinga Member|65891|5|Briefly described|p221-222.|Paleogene|Paleogene|Unit in lower Port Willunga Formation. Overlies Chinaman Gully Formation; is overlain by Ruwarung Member. Rupelian age.||||||
27074|Aldinga Member|66131|6|Mentioned|p242 Fig.2|Oligocene|Eocene|Late Eocene to Early Oligocene in age (from p.242 Fig.2 - stratigraphic correlation chart).||Unit in Port Willunga Formation.||Underlain by the Chinaman Gully Formation. Is overlain by Ruwarung Member.||
27074|Aldinga Member|67462|5|Briefly described|Map legend.|Oligocene|Eocene|Eastern Saint Vincent Basin.||Unit in Port Willunga Formation.||||
27074|Aldinga Member|68715|6|Mentioned|p31 Fig.5|Rupelian|Priabonian|St Vincent Basin.||||||
27074|Aldinga Member|70660|4|Described|p8-p9, p12, p18|Rupelian|Rupelian|A type section is briefly described but an exact location is not provided. Fossil assemblage discussed in some detail. See also p20, p21 fig 11c, p25, p32, p46.||Port Willunga Formation||Overlies the Chinaman Gully Formation. Overlain by the Ruwarung Member.|Sandstone and muddy limestone, clay, byrozoal.|
27074|Aldinga Member|70722|5|Briefly described|p217-218|Early Oligocene|Early Oligocene|Of St. Vincent Basin. Equivalent to Kingscote Limestone Units K2 and K3 of this study.||Unit of Port Willunga Formation.||Lowermost unit of port Willunga Formation. Overlain by Ruwarung Member. Underlain by Chinaman Gully Formation.||
27074|Aldinga Member|73188|6|Mentioned|p320|Oligocene|Oligocene|St Vincent Basin.||Port Willunga Formation||||
79867|Aldoona Member|64801|5|Briefly described|p111-112, p116, p119|Cryogenian|Cryogenian|New, informal name. Unconformity-bound genetic increment of strata [?]. Sediments derived from nearby exposed diapirs. In part equivalent to, or replacing the Wundowie Member of the Enorama Shale?||Enorama Shale.|||Shallow-water stromatolitic, ooid, intraclast and lithoclast limestones, overlain by deeper-water green siltstones which shallow up to stromatolitic limestone again.|21-JUN-17
79867|Aldoona Member|72473|6|Mentioned|p4|||||||||
24153|Alinerta Gravel|40925|6|Mentioned|Map legend|Cenozoic|Cenozoic|||||||19-NOV-08
24153|Alinerta Gravel|40926|3|Fully described|p32|||Mention Plate 10||||||
24153|Alinerta Gravel|41098|4|Described|p179|||||||||
24153|Alinerta Gravel|42905|5|Briefly described|p24, Fig 5.3|||||||||
33891|Alinya Formation|22506|6|Mentioned|p128|||||||||
33891|Alinya Formation|22746|5|Briefly described|Fig.3 p515|Cryogenian|Cryogenian|||||||
33891|Alinya Formation|22922|5|Briefly described|32|||||||||
33891|Alinya Formation|23282|2|Defined|p51||Neoproterozoic|Was in Pinyin Beds (Major 1973). Originally named Alinya beds. Age: Precambrian, Neoproterozoic, Willouran to Tourensian Epochs.||||||
33891|Alinya Formation|23286|3|Fully described|p89||Neoproterozoic|Large fossil assemblage.||||||
33891|Alinya Formation|23287|6|Mentioned|p102|||Of Officer Basin.||||||26-AUG-08
33891|Alinya Formation|23288|4|Described|Fig.6 p125||Neoproterozoic|see also Fig.5, 18. of Early Neoproterozoic Torrensian succession. Revised from "Alinya beds" & Alynia beds . Shale of Alinya Fm previously upper part of Pindyin beds. Full explanation of acritarch assemblage. of Officer Basin.||||||
33891|Alinya Formation|23479|5|Briefly described|p26|||Geological Province: Gawler Craton.||||||
33891|Alinya Formation|23524|5|Briefly described|p221 Fig. 3|Neoproterozoic|Neoproterozoic|||||||
33891|Alinya Formation|23557|5|Briefly described|p95 Fig.1|Cryogenian|Cryogenian|Geological Province: Officer Basin.||||||
33891|Alinya Formation|24111|5|Briefly described|p210 Fig. 4|Neoproterozoic|Neoproterozoic|Geological Province: Officer Basin.  See also p215 Fig. 11, p212.||||||
33891|Alinya Formation|24112|5|Briefly described|p254 Fig.2, p268 Tb.5|Neoproterozoic|Neoproterozoic|Of the Callanna Group. Geological Province: Officer Basin||||||
33891|Alinya Formation|44109|5|Briefly described|p17, p22 Fig. 19|Willouran|Willouran|Together with Pindyin Sandstone, forms the basal units of the Officer Basin. Geological Province: central Officer Basin.||||||
33891|Alinya Formation|61732|5|Briefly described|p4 Fig. 3, p58 Fig. 22|Willouran|Willouran|Overlain by Murnaroo Formation. Geological Province: eastern and central Officer Basin. See also p81, p131.||||||07-FEB-11
33891|Alinya Formation|62453|5|Briefly described|p5 Fig. 3, 12 Fig. 8|Cryogenian|Cryogenian|Geological Province: Officer Basin.||||||
33891|Alinya Formation|63397|6|Mentioned|5|Neoproterozoic|Neoproterozoic|||||||
33891|Alinya Formation|63811|6|Mentioned|p506|Neoproterozoic|Neoproterozoic|Present in the Giles 1 Drillhole, Officer Basin. Contains benthic cyanobacteria and acritarchs.||||||
33891|Alinya Formation|64103|6|Mentioned|p400 Fig. 3|Cryogenian|Cryogenian|Geological Province: Officer Basin.||||||07-FEB-11
33891|Alinya Formation|64325|6|Mentioned|p83|||Geological Province: eastern Officer Basin in South Australia. Correlative of Browne Formation.||||||26-AUG-08
33891|Alinya Formation|64793|6|Mentioned|p284 Fig.3, p286, p288-289|||Of Officer Basin.||||||
33891|Alinya Formation|64794|5|Briefly described|p238 fig 2, p244, p266|Cryogenian|Cryogenian|||||||
33891|Alinya Formation|65365|5|Briefly described|p10 Fig. 4|Cryogenian|Cryogenian|Eastern Officer Basin||||||
33891|Alinya Formation|65366|5|Briefly described|p23 Fig. 3|Cryogenian|Cryogenian|Eastern Officer Basin||||||
33891|Alinya Formation|65410|6|Mentioned|p72, pp76-78.|Neoproterozoic|Neoproterozoic|Officer Basin. Part of Supersequence 2. Contains a distinctive, diverse palynological assemblage. Interpreted as a sub-tidal shelf to coastal sabkha facies. Potential hydrocarbon source rock.||||||
33891|Alinya Formation|67536|6|Mentioned|Map Legend|||Mapped with Pindyin Sandstone as N3.|||||Tidal to sabkha siltstone, shale, sandstone with anhydrite.|01-APR-14
33891|Alinya Formation|68270|5|Briefly described|p683|Tonian|Tonian|Eastern Officer Basin.||||Overlain disconformably/unconformably by Chambers Bluff Tillite. Underlain by Pindyin Sandstone.||
33891|Alinya Formation|69003|6|Mentioned|p60|Neoproterozoic|Neoproterozoic|E Officer Basin.||||||
33891|Alinya Formation|69203|6|Mentioned|p59|||Officer Basin.||Callana Group.||||
33891|Alinya Formation|69648|4|Described|p17-18, p34, p36, map legend|Neoproterozoic|Neoproterozoic|Age: Willouran. Probable equivalents of this unit have been interpreted from drillhole logs. Highstand shale/siltstone contains dolomitic chert in lower part and limestone at top; evaporite minerals. Thickness: max 116m (in drilhole GOD/SAN YL2) and generally decreases to south. Prospective for evaporite minerals. Diapiric structures formed.||||Conformably overlies Pindyin Sandstone; unconformably (although structurally conformable) overlain by Tarlina Formation (major hiatus spanning ~130 my).|In drillholes, shale and calcareous shale interbedded with micritic (locally cherty, oolitic) limestone; dolomitic mudstone (some pyritic, carbonaceous) to micritic dolostone (locally stromatolitic); sandstone and anhydrite horizons common.|
33891|Alinya Formation|72478|6|Mentioned|p8, Fig 6 p69(digital)|Willouran|Torrensian|Officer Basin.|c. 800-790 Ma|Callanna Group||Overlies the Pindyin Sandstone. Overlain by the Coominaree Dolomite. Unconformably overlain by the Chambers Bluff Tillite.||29-MAR-21
33891|Alinya Formation|73099|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Officer Basin.||||Overlies Pindyin Sandstone. Is overlain by Lake Maurice Group.|Green-grey and brown, laminated claystone, siltstone and anhydrite, very fine- to very coarse-grained, feldspathic quartz sandstone, minor dolostone and halite. Diapiric source beds.|
33891|Alinya Formation|73392|6|Mentioned|p3||||||||Sampled from core of Giles 1 well.|
23328|Allendale Metasediments|6823|6|Mentioned|p205|||||Broken Hill Group||||
23328|Allendale Metasediments|22553|5|Briefly described|fig2p77,p80|Proterozoic|Proterozoic|||||||
23328|Allendale Metasediments|22575|6|Mentioned|p179 Fig.2|||Of the Broken Hill Group.||||||11-JUN-08
23328|Allendale Metasediments|22771|6|Mentioned|Table12.2p45,45|||||||||
23328|Allendale Metasediments|22857|4|Described|p45 Tb. 12.2, p390 App1 Tb.A1.1|Paleoproterozoic|Paleoproterozoic|Of the Broken Hill Group. Thickness at Mount Robe: 1000m. Geological Province: Willyama Fold Belt.||||||07-NOV-08
23328|Allendale Metasediments|22884|6|Mentioned|p45|||Geological province: Broken Hill Domain.||||||26-MAR-09
23328|Allendale Metasediments|22964|6|Mentioned|p56||Proterozoic|||||||
23328|Allendale Metasediments|22965|6|Mentioned|Fig 1||Statherian|||||||
23328|Allendale Metasediments|22966|6|Mentioned|Fig 1||Proterozoic|Rift stage of geological development.||||||
23328|Allendale Metasediments|22967|6|Mentioned|p39||Statherian|||||||
23328|Allendale Metasediments|23025|6|Mentioned|Fig1p75|||||||||
23328|Allendale Metasediments|23160|6|Mentioned|fig1|||||||||
23328|Allendale Metasediments|23223|6|Mentioned|Table.2|||||||||
23328|Allendale Metasediments|23248|5|Briefly described|Fig2p169|||||||||
23328|Allendale Metasediments|23461|5|Briefly described|p204 Fig. 3|||Of the Broken Hill Group.||||||29-MAY-07
23328|Allendale Metasediments|24307|5|Briefly described|p975|Proterozoic|Proterozoic|Of the Broken Hill Group.  Previously included in the Purnamoota Subgroup, which has been abandoned by this study.||||||29-MAY-07
23328|Allendale Metasediments|38969|4|Described|p208|||||||||
23328|Allendale Metasediments|39662|2|Defined|p423|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
23328|Allendale Metasediments|39849|6|Mentioned|Table 2|||||||||
23328|Allendale Metasediments|40822|6|Mentioned|Fig.2|||||||||
23328|Allendale Metasediments|41093|6|Mentioned|p252|||||||||
23328|Allendale Metasediments|41145|6|Mentioned|Fig.4|||||||||
23328|Allendale Metasediments|41630|6|Mentioned|p27|||See also Fig.1.3||||||
23328|Allendale Metasediments|41633|6|Mentioned|Fig.2.2|||||||||
23328|Allendale Metasediments|42261|6|Mentioned|Fig 1 P530|||||||||
23328|Allendale Metasediments|42507|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
23328|Allendale Metasediments|42527|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
23328|Allendale Metasediments|42528|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
23328|Allendale Metasediments|42529|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
23328|Allendale Metasediments|42531|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
23328|Allendale Metasediments|42537|4|Described|p13|||||||||
23328|Allendale Metasediments|42595|6|Mentioned|Fig. 2 P5|||||||||
23328|Allendale Metasediments|42813|6|Mentioned|p9|||||||||
23328|Allendale Metasediments|42897|5|Briefly described|Fig.3, P321|||||||||
23328|Allendale Metasediments|43052|6|Mentioned|Fig.4.22|||||||||
23328|Allendale Metasediments|43086|6|Mentioned|Fig.3|||||||||
23328|Allendale Metasediments|43265|5|Briefly described|Map Legend||Paleoproterozoic|Of the Broken Hill Group.||||||07-NOV-08
23328|Allendale Metasediments|43266|5|Briefly described|Map Legend||Paleoproterozoic|Of the Broken Hill Group.||||||07-NOV-08
23328|Allendale Metasediments|43270|5|Briefly described|Map Legend||Paleoproterozoic|Of Purnamoota Subgroup.||||||07-NOV-08
23328|Allendale Metasediments|43271|5|Briefly described|Map Legend||Paleoproterozoic|Of the Broken Hill Group.||||||07-NOV-08
23328|Allendale Metasediments|43272|5|Briefly described|Map Legend||Paleoproterozoic|Of the  Broken Hill Group.||||||07-NOV-08
23328|Allendale Metasediments|43274|5|Briefly described|Map Legend||Paleoproterozoic|Of the Broken Hill Group.||||||07-NOV-08
23328|Allendale Metasediments|43572|6|Mentioned|Fig.3.2 p6|||||||||
23328|Allendale Metasediments|43583|5|Briefly described|Table 1, p2139|||||||||
23328|Allendale Metasediments|46598|4|Described|p303|||||||||
23328|Allendale Metasediments|50045|4|Described|p116 Fig. 3, p115 Fig. 2|Statherian|Statherian|Geological Province: Broken Hill Block. Of the Broken Hill Group (Willyama Supergroup). Overlain by Purnamoota Subgroup; underlain by Thackaringa Group. Includes: Ettlewood Calc-Silicate Member.||||||31-MAY-07
23328|Allendale Metasediments|50619|5|Briefly described|p178 Fig. 3|Paleoproterozoic|Paleoproterozoic|Of the Broken Hill Group. Contains the Ettlewood Cal-Silicate Member. Geological Province: Broken Hill Block.||||||24-FEB-10
23328|Allendale Metasediments|60485|5|Briefly described|p30|||Of the Broken Hill Group.  Contains the Ettlewood Calc-Silicate Member.||||||
23328|Allendale Metasediments|61606|5|Briefly described|p4 Fig.2|Paleoproterozoic|Paleoproterozoic|Of the Broken Hill Group.||||||07-NOV-08
23328|Allendale Metasediments|61735|5|Briefly described|p636 Fig. 2, p638, 639|Paleoproterozoic|Paleoproterozoic|Of Broken Hill Group. Presented as Allendale only in Fig. 2. Max depositional age ~1750 Ma.||||||04-JUN-15
23328|Allendale Metasediments|61736|5|Briefly described|p666 Fig. 3|Paleoproterozoic|Paleoproterozoic|Includes Ettlewood Calc-Silicate Member. Geological province: Olary Domain.||||||24-FEB-10
23328|Allendale Metasediments|62473|5|Briefly described|p73|Paleoproterozoic|Paleoproterozoic|Of Broken Hill Group. Age: 1691+/-3Ma. Tuffaceous metasediments.||||||17-JUN-09
23328|Allendale Metasediments|62535|5|Briefly described|p666 Fig.3, p672|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain.||Broken Hill Group.|Ettlewood Calc-Silicate Member.|||
23328|Allendale Metasediments|62536|5|Briefly described|p633, 636, 638-639, 641, 646|||Broken Hill area.|c.1690 Ma. MDA of ~1750 Ma.|Broken Hill Group.|Ettlewood Calc-Silicate Member.|||
23328|Allendale Metasediments|62592|5|Briefly described|p16 Fig.2.2. |Statherian|Statherian|Broken Hill Domain, Curnamona Province.|1693 +/- 4 Ma.|Unit in Broken Hill Group.||||
23328|Allendale Metasediments|62993|6|Mentioned|p37|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain.||Broken Hill Group|Includes Ettlewood Calc-Silicate Member|||19-DEC-21
23328|Allendale Metasediments|63102|5|Briefly described|p13-14,26,32|||Geological province: Broken Hill Domain, Curnamona Province.||Unit of Broken Hill Group.|Includes Ettlewood Calcasilicate Member.|||
23328|Allendale Metasediments|63519|5|Briefly described|p5, p6 Fig. 2|Paleoproterozoic|Paleoproterozoic|Of the Paragon Group. Include the Ettlewood Calc-Silicate Member. See also p10 Fig. 3,  p29 Fig. 11..||||||07-NOV-08
23328|Allendale Metasediments|63866|5|Briefly described|p36, p38|||Broken Hill Domain, Curnamona Province. ||Broken Hill Group|Includes the Ettlewood Calc-Silicate Member.|Overlain by the Parnell Formation.|Thin bedded pelite to psammopelite with minor mafic gneiss and calc-silicate nodules.|
23328|Allendale Metasediments|64097|5|Briefly described|p302 Tb.1, p303 Fig. 2|||Of Broken Hill Group. Contains Ettlewood Calc-Silicate Member.||||||07-FEB-11
23328|Allendale Metasediments|64316|5|Briefly described|p533 Fig. 1|Paleoproterozoic|Paleoproterozoic|Of Broken Hill Group (Willyama Supergroup). Geological Province: Broken Hill Block.||||||07-FEB-11
23328|Allendale Metasediments|64741|5|Briefly described|p301 Fig. 4, p309|Paleoproterozoic|Paleoproterozoic|Of Broken Hill Gp. Contains Ettlewood Calc-Silicate Mbr. Overlain by Parnell Gneiss. Geol.prov: Broken Hill Domain. Lower pelitic unit (very minor psammite) and upper, dominantly siliciclastic facies, with finely bedded pelites + minor thin psammites.||||||07-FEB-11
23328|Allendale Metasediments|64742|6|Mentioned|p321 Fig.3, P323. |||||Unit in Broken Hill Group.|||Albitic psammite, pelite.|
23328|Allendale Metasediments|64944|5|Briefly described|p29 Tb.1|Paleoproterozoic|Paleoproterozoic|Of Broken Hill Group. Equivalent to Plumbago Formation in the Olary Domain. Geological province: Broken Hill Domain.||||||07-FEB-11
23328|Allendale Metasediments|66302|4|Described|p36 Fig.9, p39, p40|Statherian|Statherian|Broken Hill Domain, Curnamona Province. ||Broken Hill Group|Includes the Ettlewood Calc-silicate Member.|Overlies the Himalaya Formation. Overlain by the Purnamoota Subgroup, Parnell Gneiss.|Thin-bedded mudstone to siltstone with minor mafic gneiss and calc-silicate nodules.|
23328|Allendale Metasediments|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Broken Hill Domain.|1693 +/- 3 Ma.|Broken Hill Group.|Ettlewood Calc-Silicate Member.|||
23328|Allendale Metasediments|70000|5|Briefly described|p34, p36|Statherian|Statherian|||Unit in Broken Hill Group.|Includes Ettlewood Calc-Silicate Member.|Is overlain by Purnamoota Subgroup.|Siliciclastic, pelite-dominated rocks.|
23328|Allendale Metasediments|70014|5|Briefly described|Map legend|||||Basal unit in Broken Hill Group.|Includes Ettlewood Calc-Silicate Member.|Overlies Rasp Ridge Gneiss and Himalaya Formation (Broken Hill Group). Is overlain by Purnamoota Subgroup.|Mainly metasediment and metasedimentary composite gneiss. Variable ratio of pelite:psammopelite:psammite. Commonly garnet-rich. Sproradic bodies of basic gneiss and quartz-gahnite, quartz-iron sulfide. Sporadic zoned calc-silicate nodules.|07-SEP-15
23328|Allendale Metasediments|70015|5|Briefly described|Map legend|Statherian|Statherian|Mineral deposits (if any) are shown.||Unit in Broken Hill Group.||Overlies Himalaya Formation.|Pelitic to psammitic metasedimentary composite gneiss, including garnet-bearing feldspathic composite gneiss, sporadic basic gneiss and quartz-gahnite rock. Calc-silicate bodies at base.|07-SEP-15
23328|Allendale Metasediments|70405|6|Mentioned|p40, p43 table 3|Paleoproterozoic|Paleoproterozoic|||Broken Hill Group||||
23328|Allendale Metasediments|70657|4|Described|p13 Fig.6, p14-17, p34, p37, p39|Statherian|Statherian|Curnamona Province: Broken Hill Domain. (Stevens et al, in prep). With Ettlewood Calc-Silicate Member, is equivalent to Larry Macs Subgroup (Saltbush Group) of Olary Domain.|~1700-1685 Ma|Broken Hill Group|Includes Ettlewood Calc-Silicate Member.|Underlies Purnamoota Subgroup. Overlies Himalaya Formation (Thackaringa Group). Intruded by Stephens Creek Granite Gneiss and Wondervale Well Granite Gneiss, of the Silver City Suite.||
23328|Allendale Metasediments|70658|5|Briefly described|p7, 15, 47|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain, Curnamona Province.||Broken Hill Group.||Locally overlies Plumbago Formation.||
23328|Allendale Metasediments|72461|5|Briefly described|p16 fig 9, p17|||||Broken Hill Group|Includes the Ettlewood Calc-silicate Member.|Overlies the Himalaya Formation. Ovderlain by the Parnell Gneiss.||
23328|Allendale Metasediments|73243|6|Mentioned|p52 Fig.1|Statherian|Statherian|Broken Hill block-Euriowie block.||Broken Hill Group|Ettlewood CS|||
23328|Allendale Metasediments|73308|6|Mentioned|p607 Fig.1|||||Broken Hill Group.|Ettlewood Calc-Silicate Member.|||
23328|Allendale Metasediments|73429|5|Briefly described|p106 Fig.2|Statherian|Statherian|Curnamona Province, Broken Hill Domain.||Broken Hill Group|Ettlewood Calc-Silicate Member|Underlies Purnamoota Subgroup||
23328|Allendale Metasediments|73482|6|Mentioned|p422 Fig.3|||||Broken Hill Group|Ettlewood CS|||
23328|Allendale Metasediments|73512|6|Mentioned|p2|||||||||
23328|Allendale Metasediments|73524|6|Mentioned|p5 Fig.3|||||Broken Hill Group||||
23328|Allendale Metasediments|73575|5|Briefly described|p828 Fig.2, p829 Fig.3, p831 Fig.5|Statherian|Statherian|||Broken Hill Group|Ettlewood Calc-Silicate Member|Overlies Himalaya Formation, underlies Purnamoota Subgroup, Parnell Formation||
23330|Alpana Formation|39904|2|Defined|p9|Late Paleozoic|Late Paleozoic|||||||07-NOV-08
23330|Alpana Formation|43053|5|Briefly described|Map Legend|Permian|Carboniferous|Glaciomarine and fluvioglacial sediments, including diamictite.||||||25-MAY-05
23330|Alpana Formation|43298|6|Mentioned|Map Legend|Permian|Carboniferous|||||||
23330|Alpana Formation|44133|5|Briefly described|p65 Fig. 8.4, 90|Permian|Carboniferous|Unconformably overlies Callana Group. ~20m thick.||||||
23330|Alpana Formation|60953|5|Briefly described|Map legend|Permian|Carboniferous|Glaciomarine and fluvioglacial sediments, including diamicite.||||||
23330|Alpana Formation|60959|5|Briefly described|Map Legend|Permian|Carboniferous|Till with polished, faceted and striated clasts; proglacial sand with small amounts of gravel and lonestones.||||||11-MAY-05
23330|Alpana Formation|61108|5|Briefly described|map legend|Permian|Carboniferous|Glaciomarine, fluvioglacial and fluviolacustrine till, clay, silt, sand and gravel, indurated and coal-bearing in Ackaringa Basin.||||||02-JUN-05
23330|Alpana Formation|65376|6|Mentioned|p47, p92 Fig. 2.82, p229 Fig.6.39.|Permian|Carboniferous|||||||
23330|Alpana Formation|73129|6|Mentioned|p46 Fig.5|Triassic|Pennsylvanian|||||||09-JUN-22
69205|Alpha Mudstone|60564|5|Briefly described|p4, p5|||Overlies the Bulldog Shale. Thickness: >100m. Dense plastic clay.||||||
69205|Alpha Mudstone|65194|6|Mentioned|p36-37, p47|||Curnamona Province. Lower unit in Namba Formation. Contains the Beverley Palaeochannel aquifer: no indirect lateral recharge results in rapid and sustained storage depletion following abstraction. Dark-brown to black clay; minor oxidised yellow-brown bands and black organic matter.||||||
69205|Alpha Mudstone|65925|5|Briefly described|p17, pp57-59, p65.|Miocene|Oligocene|Contains plant fragments and carbonised wood. Sinuous sand-filled depressions in upper surface host much of Beverley U deposit.||Basal unit in Namba Formation.|||Mudstone with organic material.|
69205|Alpha Mudstone|67202|6|Mentioned|p252 Fig.7.17|||Beverley, SA. Infill in a palaeosurface drainage channel; associated with uranium mineralisation.||||||
69205|Alpha Mudstone|69562|6|Mentioned|p662 Tb.2, p675|||Extremely low permeability. Enriched in carbonaceous matter which could act as reductant for U deposits. Electrical conductivity value used in forward modelling: 600 mS/m.||Unit in Namba Formation.||Is overlain by Beverley Sands.||
35893|Ameroo Subsuite|23347|2|Defined|p53 Fig. 3, p55|Statherian|Statherian|Of the Basso Suite (Willyama Supergroup.) Age: 1711+/-2Ma. Intrusive member of the Basso Suite. Metagranite previously named Basso Granodiorite.||||||24-FEB-10
35893|Ameroo Subsuite|62728|5|Briefly described|p28|Paleoproterozoic|Paleoproterozoic|Granitoid component of Basso Suite. Consists of foliated biotite gneiss or adamellite gneiss. A-type. Age: 1711+/-2Ma (U-Pb, Page et al, 1998). Geological Province: Olary Domain/Curnamona Province.||||||07-FEB-11
35893|Ameroo Subsuite|62993|6|Mentioned|p8|Paleoproterozoic|Paleoproterozoic|||Basso Suite||||
35893|Ameroo Subsuite|63102|4|Described|p35,39|Statherian|Statherian|Geological province: Olary Domain, Curnamona Province. Thickness of sills: tens to few hundreds of meters. A-type igneous magmatism coeval with Curnamona Group sedimentation i.e. Montstephen Basalt. Reported U-Pb zircon results include Ameroo Hill (1703+\-6 Ma), Poodla Dam (1717+\-14 Ma), Drew Hill body north of Mount Mulga Barite Mine (1701+\-8 Ma) (Ashley et al., 1996), and the Drew Hill body east of the Mt Mulga Barite Mine (~1711+\-2 Ma; Page et al., 1998).|1711+\-2 Ma|Unit of Basso Suite.|||Extrusives, possible thin subvolcanic sills, and proximal volcaniclastics. Metagranites: albite + quartz with lesser Kfeldspar, biotite, muscovite and magnetite, and traces of zircon and xenotime.|
35893|Ameroo Subsuite|64944|5|Briefly described|p27|Paleoproterozoic|Paleoproterozoic|Of Basso Suite. Age: ~1711Ma.||||||07-FEB-11
35893|Ameroo Subsuite|66302|5|Briefly described|p36 Fig.9|Statherian|Statherian|Olary Domain, Curnamona Province|ca. 1713-1711 Ma|Basso Suite|||Granitic sills.|
35893|Ameroo Subsuite|67540|5|Briefly described|p29 Tb.2|Statherian|Statherian||~1710 Ma|?Of the lower Willyama Supergroup.||Intruded by the Triangle Hill Granite.|Metagranites.|03-FEB-16
35893|Ameroo Subsuite|68126|5|Briefly described|p31|Paleoproterozoic|Paleoproterozoic||1715-1710 Ma.||||Albitic A-type metagranitoid with local gneissic layering and minor biotite. Leucocratic quartz-feldspar gneiss with coarse biotite.|
35893|Ameroo Subsuite|69650|5|Briefly described|p5, p19|Paleoproterozoic|Paleoproterozoic||c.1710 Ma.|||Intruded by Triangle Hill Granite.|Metagranites.|
35893|Ameroo Subsuite|70340|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic||1715-1710 Ma||||Metagranitoid, locally foliated; biotite gneiss; adamellite gneiss. A-type. Essentially concordant.|
35893|Ameroo Subsuite|70405|4|Described|p35|Paleoproterozoic|Paleoproterozoic|May be difficult to differentiate from metasedimentary albitites.|1710 Ma - 1720 Ma|Basso Suite||Intrudes into George Mine Formation|Medium-coarse grained Metagranites  with strong gneissic foliation especially in biotite rich metagranites. Albitic granites are generally biotite poor and less foliated.|
35893|Ameroo Subsuite|70657|5|Briefly described|p16, p33, p45-46|Statherian|Statherian|Curnamona Province. Sills range from tens to few hundreds of metres thick. This age range (Page et al., in prep.) approximates the earliest zircon grains of the Redan Gneiss.|1713 +/- 5 Ma - 1711 +/- 2 Ma.|Basso Suite.|||Metagranites; commonly as thick sills, and coarsely crystalline. Generally foliated or lineated. A-type.|
35893|Ameroo Subsuite|70658|5|Briefly described|p1-2, 5-7, 15, 18, 23, 29, 32|Paleoproterozoic|Paleoproterozoic|Olary Domain, Curnamona Province. Geochemistry briefly described.|~1712 Ma.|Basso Suite.|||Voluminous A-type metagranite.|
26343|Ampeinna Granite|30923|6|Mentioned|Map legend|early Adelaidean|early Adelaidean|||||||
26343|Ampeinna Granite|50607|5|Briefly described|p2.2|||Geological Province: Musgrave Block. Of the Southern granites Suite (Kulgera Supersuite).||||||
26344|Anabama Granite|22631|6|Mentioned|p178|||||||||
26344|Anabama Granite|23351|6|Mentioned|283|||||||||
26344|Anabama Granite|23818|5|Briefly described|p34 Fig.8, p106|Ordovician|Ordovician|Geological Province: Willyama Block. Age: 473 Ma.||||||
26344|Anabama Granite|23869|5|Briefly described|p16|||Age: Delamerian||||||
26344|Anabama Granite|24509|6|Mentioned|p41 Fig. 2b|Ordovician|Cambrian|Geological Province: Murray Basin.||||||
26344|Anabama Granite|30398|6|Mentioned|p259|||||||||
26344|Anabama Granite|30513|6|Mentioned|p46|||||||||
26344|Anabama Granite|30808|6|Mentioned|Fig.1|||||||||
26344|Anabama Granite|30810|6|Mentioned|Fig.1|||||||||
26344|Anabama Granite|33468|6|Mentioned|p209|||||||||
26344|Anabama Granite|33490|5|Briefly described|p11|||Delamerian c.470my||||||
26344|Anabama Granite|33845|6|Mentioned|p436|||Absolute age||||||
26344|Anabama Granite|34537|6|Mentioned|Fig.8|||Ord.||||||
26344|Anabama Granite|34612|6|Mentioned|p106|||Lower Ordovician. 473 my.||||||
26344|Anabama Granite|35358|6|Mentioned|p18|||Age dating||||||
26344|Anabama Granite|36833|4|Described|p6|||||||||
26344|Anabama Granite|38068|5|Briefly described|p69|||||||||
26344|Anabama Granite|40642|6|Mentioned|p173|||||||||
26344|Anabama Granite|41403|6|Mentioned|p54|||||||||
26344|Anabama Granite|42098|4|Described|p54|||||||||
26344|Anabama Granite|42222|6|Mentioned|p26|||||||||
26344|Anabama Granite|42274|6|Mentioned|p458|||||||||
26344|Anabama Granite|42720|5|Briefly described|map legend|Ordovician||||||||
26344|Anabama Granite|42813|4|Described|p22|||age of 458 Ma||||||
26344|Anabama Granite|44133|6|Mentioned|p54, 56 Table 7.3|Late Ordovician|Middle Ordovician|Coarse-grained biotite granite to granodiorite. S-Type to marginally I-Type. Age: 455 +/- 7Ma, 463 +/- 3, 458 +/- 62, 450Ma.||||||
26344|Anabama Granite|48894|6|Mentioned|p74|||437+-3my||||||
26344|Anabama Granite|73093|5|Briefly described|map legend|Ordovician|Cambrian||||||Granite to granodiorite, coarse-grained, biotitic. S-type to ?I-type.|09-DEC-21
34744|Anama Siltstone Member|22889|2|Defined|p33 & p38|Adelaidean|Adelaidean|Location of Type Section given on p38.||||||
34744|Anama Siltstone Member|70819|5|Briefly described|p18|Neoproterozoic|Neoproterozoic|Clare Valley. Represents a marine transgression over the fluvial deposits of the parent unit.||Rhynie Sandstone.||Is overlain gradationally by Blyth Dolomite.|A succession of carbonaceous siltstones and shales with interbeds of sandstone, arkosic grit, and minor dolomite.|
28124|Angaston Marble|23275|6|Mentioned|p472|||||||||
28124|Angaston Marble|30051|6|Mentioned|Fig.1|||||||||
28124|Angaston Marble|30801|6|Mentioned|p5|||See also P6. Table. Lower Cambrian age.||||||
28124|Angaston Marble|30807|6|Mentioned|p102|||Suggested map symbol||||||
28124|Angaston Marble|32547|6|Mentioned|Fig.2|||L.Camb. unit of Hawker Group||||||
28124|Angaston Marble|34536|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
28124|Angaston Marble|34615|6|Mentioned|p7|||Shown on Figure.||||||
28124|Angaston Marble|34959|5|Briefly described|p284|||||||||
28124|Angaston Marble|40003|5|Briefly described|Table 4|||||||||
28124|Angaston Marble|40499|6|Mentioned|p152|||||||||
28124|Angaston Marble|40852|6|Mentioned|Table 3.1|||||||||
28124|Angaston Marble|40856|5|Briefly described|p312|||Mention Fig.23.6||||||
28124|Angaston Marble|42222|6|Mentioned|Table 1 P4|||||||||
28124|Angaston Marble|44133|5|Briefly described|p18|||Of the Normanville Group. ||||||
28124|Angaston Marble|61307|5|Briefly described|p6 Fig. 3|Cambrian|Cambrian|Of the Normanville Group. Geological Province: Karinya Syncline/Adelaide Fold Belt.||||||
28124|Angaston Marble|65379|5|Briefly described|p643, p644, p647|Cambrian|Cambrian|Of Normanville Group, Moralana Supergroup. Marble, coarse-grained, amphibolitic, white, crystalline. N.B. Asbestos deposit host, contains Dutton 1 asbestos prospect and other asbestos occurrences.||||||07-MAR-12
33655|Angatja Granite|60572|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Age: ~1070Ma?||||||17-JUL-06
33655|Angatja Granite|60683|2|Defined|p54 Appendix, p19-20|Mesoproterozoic|Mesoproterozoic|Of Angatja Granite Suite. Synonymous with part of Musgrave-Mann Metamorphics of Thomson (1969) and undivided metamorphosed granites of Forman (1972).  A suite of charnockite, hornblende granite and rapakivi granite. Age: c.1070Ma.  See also p9 Tb.1, p42.||||||23-DEC-09
33655|Angatja Granite|61154|4|Described|p14, p13, p42,42 in Appendix|Mesoproterozoic|Mesoproterozoic|See also Angatja Suite. Includes charnockite, hornblende granite and rapakivi granite; the granite is dominantly porphyritic. Intrudes the Alcurra Dolerite in the eastern Mann Ranges. Age: 1071+/-5Ma (Scrimgeour et al 1999). Geol. Province: Musgrave Block||||||14-JUL-05
33655|Angatja Granite|61386|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Porphyritic orthopyroxene-clinopyroxene granite (locally with rapakivi textures) and coarsely porphyritic hornblende-biotite granite; both variably mylonitised and recrystallised.  Age: ~1070Ma. Geological Province: Musgrave Block.||||||
33655|Angatja Granite|61524|5|Briefly described|p18 Fig.2(a)|||Geological Province: Musgrave Province.||||||
33655|Angatja Granite|61864|6|Mentioned|p19 fig 5|||Granite intrusion and associated dykes related to the Giles Complex.||||||
33655|Angatja Granite|63866|5|Briefly described|p207|Stenian|Stenian|Fregon Domain, Musgrave Province.|1071 +/- 5 Ma (Scrimgeour et al, 1999)|||||
33655|Angatja Granite|65256|6|Mentioned|p15|Stenian|Stenian|Correlated with Hull Granite Suite; 1071+/-5 Ma.||||||
33655|Angatja Granite|67128|5|Briefly described|p3, p27-28|||Eastern Mann Ranges. Strongly deformed during the Petermann Orogeny.|1071 +/- 5 Ma (Scrimgeour et al., 1999).||||Mesocratic, K-feldspar porphyritic to rapakivi-textured, hornblende-orthopyroxene-biotite-garnet bearing granite.|
33655|Angatja Granite|67536|5|Briefly described|Map Legend|Stenian|Stenian|Musgrave Block.|ca. 1070 Ma||||Massive granite; weakly magnetic.|
33655|Angatja Granite|69436|5|Briefly described|p21:11|Mesoproterozoic|Mesoproterozoic|Scrimgeour et al. (1999). Kober Pb-Pb zircon age of granite.|1071 +/- 5 Ma (Scrimgeour et al., 1999).|Angatja Suite.|||Coarsely porphyritic hornblende granite; contains coarse ellipsoidal pale-blue K-feldspar phenocrysts, elongated in the fabric; mafic minerals constitute 20-25% of the rock.|12-JUL-16
33655|Angatja Granite|71592|5|Briefly described|Appendix A.|||Musgrave Province. Age determination by zircon Pb-Pb evaporation.|1071+/-5 Ma (crystallisation).||||Granite.|
42420|Angatja Suite|24496|5|Briefly described|p14|Mesoproterozoic|Mesoproterozoic|See also Angatja Granite Suite. Granitoids.  Geological Province: Musgrave Block.||||||
42420|Angatja Suite|60679|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Porphyritic granite, coarsely porphyritic granite. Geological Province: Musgrave Block.||||||14-JAN-05
42420|Angatja Suite|60683|6|Mentioned|p10 Tb. 1|||Informal abbreviation of Angatja Granite Suite?||||||
42420|Angatja Suite|61154|5|Briefly described|p12, p28|Mesoproterozoic|Mesoproterozoic|See also Angatja Granite Suite. Age: 1071+/-5Ma.||||||17-JUL-06
42420|Angatja Suite|69436|4|Described|p21:11-12, 14|Mesoproterozoic|Mesoproterozoic|After Angatja Granite (Scrimgeour et al., 1999). Musgrave Province. Emplaced during the Giles Event (1085-1040 Ma). Believed to be genetically related to the Giles Complex. Kober Pb-Pb zircon age of granite.|1071 +/- 5 Ma (Scrimgeour et al., 1999).|Warakurna Supersuite.|Angatja Granite.|Intrudes Alcurra Dolerite and Musgravian gneiss. Is intruded by Kullal Dyke Suite.|Charnockite, dark, overprinted with mylonitic fabric; coarsely porphyritic hornblende granite, with pale blue K-feldspar phenocrysts elongated in the fabric; and rapakivi granite bodies forming fine-grained dykes with coarse K-feldspar crystals.|12-JUL-16
42420|Angatja Suite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||charnockite, granite|
28203|Angepena Formation|22510|1|Redefined|table1p37, p40|||Of the Upalinna Subgroup.  Age: Marinoan. Redefined to include former upper members of Brighton Limestone and Balcanoona Formation.||||||13-OCT-04
28203|Angepena Formation|22631|6|Mentioned|p178|||Age: Marinoan||||||05-JUL-13
28203|Angepena Formation|23054|5|Briefly described|p14-5|||||||||
28203|Angepena Formation|23250|5|Briefly described|p1124 Fig.2||Cryogenian|Actually referred to as Angepena Formation equivalent -- this equivalent correlating with Etina Formation, Sunderland Formation (Umberatana Group) and Aralka Formation, Limbla Member and Ringwood Member.||||||24-JUN-09
28203|Angepena Formation|23394|5|Briefly described|Map legend|Proterozoic|Proterozoic|||||||
28203|Angepena Formation|23445|6|Mentioned|p437|||||||||
28203|Angepena Formation|23719|5|Briefly described|p26|Neoproterozoic|Adelaidean|Of Willochra Subgroup. Geological Province: Gawler Craton.||||||24-JUN-09
28203|Angepena Formation|23818|4|Described|p64 Fig.22, p70|Adelaidean|Adelaidean|Lowermost unit of the Willochra Sub-Group. Underlain by Balcanoona Formation. Max. thickness: ~3000 ft.||||||24-JUN-09
28203|Angepena Formation|24176|4|Described|p12, p24 Tb. 1|Adelaidean|Adelaidean|Of Willochra Sub-Group (Umberatana Group).  Overlain by Elatina Formation.  Intertongues with Amberoona Formation.  Age is Marinoan.  Max. thickness: 1330m.  Geological Province: Mount Painter Province.||||||
28203|Angepena Formation|30176|6|Mentioned|Map legend|Precambrian|Precambrian|Sturtian||||||
28203|Angepena Formation|30177|2|Defined|p130|Adelaidean|Adelaidean|See also p83. Type section: Approximately four miles west of Arkaroola track, lat. 30degrees24'15"S long. 139degrees21'08"E to lat. 30degrees24'37S" long. 139degrees22'20"E thence lat. 30degrees27'43"S long.139degrees18'47"E to lat. 30degrees27'29"S long. 139degrees18'26"E.||||||25-NOV-22
28203|Angepena Formation|30801|6|Mentioned|p5|||See also P6. Table.||||||
28203|Angepena Formation|30807|6|Mentioned|p103|||Suggested map symbol||||||
28203|Angepena Formation|31797|6|Mentioned|Fig. 2|||Adelaidean. Yudnamutana Sub-Gp.||||||
28203|Angepena Formation|32506|6|Mentioned|Fig.1|||||||||
28203|Angepena Formation|32724|6|Mentioned|Fig.1|||Correlation. Marinoan||||||
28203|Angepena Formation|33422|6|Mentioned|Map legend|Precambrian|Precambrian|||||||
28203|Angepena Formation|33423|4|Described|p13|||||||||
28203|Angepena Formation|33474|6|Mentioned|Fig.2|||||||||
28203|Angepena Formation|34521|5|Briefly described|p156|||Suitable for road-making.||||||24-JUN-09
28203|Angepena Formation|34535|4|Described|p70|||See Fig.22. Marinoan||||||
28203|Angepena Formation|34536|6|Mentioned|Map legend|Adelaidean|Adelaidean|Equiv.Marinoan||||||
28203|Angepena Formation|34766|6|Mentioned|p58|||||||||
28203|Angepena Formation|35255|6|Mentioned|Fig.7|||||||||
28203|Angepena Formation|35675|6|Mentioned|p31|||||||||
28203|Angepena Formation|35678|6|Mentioned|p65|||Summary geological logs.||||||
28203|Angepena Formation|36137|4|Described|p14|||Palaeomagnetism discussed.||||||
28203|Angepena Formation|36733|6|Mentioned|Table 5|||||||||
28203|Angepena Formation|37461|4|Described|p341|||See also Table 5.I||||||
28203|Angepena Formation|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Marinoan||||||
28203|Angepena Formation|39351|6|Mentioned|Map legend|Adelaidean|Adelaidean|Marinoan||||||
28203|Angepena Formation|40254|6|Mentioned|p284|||||||||
28203|Angepena Formation|41405|3|Fully described|p177|||||||||
28203|Angepena Formation|42090|5|Briefly described|p25|||||||||
28203|Angepena Formation|42098|5|Briefly described|Table 2 P54|||||||||
28203|Angepena Formation|42222|6|Mentioned|p17|||||||||
28203|Angepena Formation|42779|5|Briefly described|Table 1 P287|||||||||
28203|Angepena Formation|42882|5|Briefly described|Fig.7 P12|||of Umberatana Group||||||
28203|Angepena Formation|43052|5|Briefly described|p189,Table 6.1|||of Willochra Subgroup||||||
28203|Angepena Formation|44289|5|Briefly described|Map Legend||Proterozoic|||||||
28203|Angepena Formation|60959|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Of the Upalinna Subgroup. Finely laminated red-brown to purple siltstone with mudcracks; dolomitic interbeds.||||||
28203|Angepena Formation|61732|5|Briefly described|p28 Fig. 13|Marinoan|Marinoan|Of the Upalinna Subgroup (Umberatana Group). Geological Province: Adelaide Rift Complex.||||||07-FEB-11
28203|Angepena Formation|62428|5|Briefly described|p351 Tb. 6|Neoproterozoic III|Neoproterozoic III|Age: 724+/-40Ma (Rb-Sr). Palaeomagnetic data.||||||10-FEB-09
28203|Angepena Formation|62592|5|Briefly described|p58.|||Benagerie Ridge area. ||||Gradationally overlies conglomerates of Upalinna Subgroup.|Redbeds.|
28203|Angepena Formation|64846|5|Briefly described|p197 Fig.2 |Cryogenian|Cryogenian|||Of the Upalinna Subgroup.||||
28203|Angepena Formation|65493|6|Mentioned|p917, p908 Fig 1|Cryogenian|Cryogenian|Of the Umberatana Group. Previously included Wundowie Limestone Member.||||||
28203|Angepena Formation|65925|5|Briefly described|Appendix 2.||||||||Siltstone, reddish, thin bedded; interbeds of dolomite and minor grey-green shale; pisolitic and algal limestone.|
28203|Angepena Formation|67030|6|Mentioned|p409 Fig. 2|Cryogenian|Cryogenian|Shown as lateral equivalent to Tarcowie Siltstone.||Willochra Subgroup||Overlies Brighton Limestone, underlies Wilmington Formation.||26-APR-12
28203|Angepena Formation|67180|4|Described|p600-612 |Cryogenian|Cryogenian|552m thick. Sturtian-Marinoan boundary placed where the red-bed sediments of this formation are first encountered. Gradational basal contact with two discrete interbeds of the Balcanoona Formation. Low-energy peri-tidal mudflat type deposit - considered shallow coastal facies situated behind the platform margin and backreef facies of the Balcanoona Formation.||Unit in Nepouie Subgroup||Conformably overlies, interbedded with and laterally equivalent to the Balcanoona Formation; unconformably overlain by the Weetootla Dolomite.|Interbedded red dolomitic mudstones and buff stromatolitic and pink dolomites. Finely laminated dolomitic muds, carbonate beds, calcareous/dolomitic and silty shales, oolitic grainstones, rip-up clasts, tepees and mudcracks, intraclastic breccias.|
28203|Angepena Formation|67870|5|Briefly described|p9|Neoproterozoic|Neoproterozoic|Adelaide Rift System.||Upalinna Subgroup.||||
28203|Angepena Formation|67979|4|Described|p528, p530 Fig.1, p531 Fig.2, p541|Sturtian|Sturtian|In Northern Flinders Ranges, the Sturtian-Marinoan Series boundary is found to coincide with an erosion surface which directly overlies the lateral and partly time-equivalent Angepena,  Balcanoona, and Tapley Hill Formations.||Nepouie Subgroup||Said to overlie Balcanoona Formation in Nepouie Creek area (Preiss et al. 1998); unconformably overlain by Weetootla Dolomite Member (in Fig.2).|shallow marine platform carbonates|
28203|Angepena Formation|69023|5|Briefly described|p70|Neoproterozoic|Neoproterozoic|Stuart Shelf. Similar stratigraphic position to Yankaninna Formation. Maximum isochron age; Webb and Coats (1980), Preiss et al. (1998).|724 +/- 40 Ma (Rb-Sr whole rock).|||||23-JAN-19
28203|Angepena Formation|70021|5|Briefly described|p97-98|Neoproterozoic|Neoproterozoic|Represents the most shoreward facies of the Oodnaminta Reef Complex. Peritidal environment.||||Lateral equivalent of Balcanoona Formation.|Mainly dolomites (oolitic, intraclastic and micritic Fe-rich carbonate) and dolomitic shales with abundant hematite. Contains abundant mud cracks and tepee structures.|
28203|Angepena Formation|70031|4|Described|p243-251|Cryogenian|Cryogenian|Adelaide Geosyncline. Thickness: less than 4km. Upper interglacial succession in the W and NE Flinders Ranges.||Unit of Upalinna Subgroup.||Intertongues with Etina Formation. Underlain conformably (SB) by Brighton Limestone/Nepouie Subgroup.|Tepee-bearing dolostone (210 m) grading upwards to rippled and mudcracked red siltstone and sandstone with thin interbeds of pink, red and grey dolostone.|
28203|Angepena Formation|70082|5|Briefly described|p2-3|Cryogenian|Cryogenian|Kulpara-Adelaide region, with equivalents in the Stuart Shelf. Contains red beds.||||Underlain unconformably by Tapley Hill Formation.||
28203|Angepena Formation|70323|6|Mentioned|p221|||Adelaide Geosyncline. Contains moderately iron-oxide-rich sediments.||||||
28203|Angepena Formation|70333|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic||||||Siltstone, reddish, thin-bedded; interbeds of dolomite and minor grey-green shale; pisolitic and algal limestone.|
28203|Angepena Formation|70334|4|Described|p2,20,23-26,38,47,50-53,77,79|Ediacaran|Ediacaran|Geological province: Gawler Craton. Of Adelaide Geosyncline and Stuart Shelf. Restricted to the eastern Stuart Shelf. Thickness: 2-50m on CULTANA. Transgressive-regressive sequence. Deposited in a shallow water oxidising environment with intermittent exposure, and coarser detritus was brought in by storm waves (Preiss, 1987). Deformed by Cambrian-Ordovician Delamarian Orogeny (~515-480 Ma). Contains a basal dolomitic member deposited in a supratidal mud flat environment (Preiss, 1987). Basal conglomerates contains clasts derived of dolomite, BIFS and sandstone from Pandurra Formation, felsic volcanics from Gawler Range Volcanics.||Unit of Upalinna Subgroup.||Conformably overlain by Wilmington Formation. Underlain by Brighton Limestone. Intertongues with Etina Formation.|Grey-green to red-brown fine-grained siltstone interbedded with medium-grained sandstone, coarse-grained lithic sandstone and lesser dolomite; gritty basalt conglomeratic beds.|14-OCT-19
28203|Angepena Formation|70384|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Adelaide Geosyncline.  Age shown more specifically as Marinoan [Cryogenian].||Of Upalinna Subgroup.||Is overlain unconformably by Weetootla Dolomite Member.|Reddish, thin-bedded siltstone; interbeds of dolomite and minor grey-green shale; pisolitic and algal limestone.|23-JAN-19
28203|Angepena Formation|71129|5|Briefly described|p15,107,110-111,114,116-117,126,208|Cryogenian|Cryogenian|Of Adelaide Geosyncline. Clastic sedimentation in a shallowing rift during Marinoan Epoch. Typically contains clasts of Pandurra Formation and Gawler Range Volcanics. Only several meters thick in drillholes in SIX MILE HILL. Deposition in a marginal marine tidal flat environment was suggested (Preiss, 1987).||||Overlain by Wilmington Formation. Correlable with Augusta Shale.|Laminated siltstone-shale succession. Calcareous, arenaceous sequence of dolomite, dolomitic greywacke and calcarenite.|13-NOV-19
28203|Angepena Formation|71895|6|Mentioned|APP4. p4, |||Punt Hill Region.||||||
28203|Angepena Formation|72247|5|Briefly described|p41,43|Neoproterozoic|Neoproterozoic|Of Adelaide Geosyncline.||||Overlain by Elatina Formation. Underlain by Brighton Limestone. Transitional to Whyalla Sandstone.||
28203|Angepena Formation|72450|5|Briefly described|Brochure, Brochure map|||Exposed in Waterfall Creek, Lonsdale railway overpass and Old Noarlunga. Deformed by the Delamerian Orogeny.||Umberatana Group|||Rippled, mud-cracked, red siltstone; fine-grained sandstone.|
28203|Angepena Formation|72613|5|Briefly described|p1-5, p8, p10-12, p14-17|Cryogenian|Cryogenian|Shown as latest Sturtian age. Records deposition in a peritidal environment equivalent to the landward of the Balcanoona reef Complex. Shales and carbonates are strongly enriched in iron oxides and represent the oldest red bed succession of the Adelaide Fold belt. The type section occurs near Arkaroola; measured sections are mentioned but no locations are given [shown in Fig.1]. Lithology and petrogrpahy in various areas are discussed in detail.|ca. 650 Ma|Umberatana Group||Laterally equivalent (in part) to the Balcanoona Formation. Shown as unconformably overlain by Yankaninna Formation.|Iron-rich marine bed succession of red mudcracked dolomitic shales, tepee dolostone, cross-bedded intraclastic ooid grainstone.|
28203|Angepena Formation|73110|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic||||||Siltstone, reddish, thin-bedded; interbeds of dolomite and minor grey-green shale; pisolitic and algal limestone.|
28203|Angepena Formation|73188|5|Briefly described|p316, p330, p333-334|Neoproterozoic|Neoproterozoic|Mount Lofty Ranges.||Upalinna Subgroup, Umberatana Group|||Red rippled and mud-cracked siltstone.|
28203|Angepena Formation|73226|6|Mentioned|p3|||Includes sandflat facies.|||||Includes laminated to flaser bedded to ripple cross-bedded siltstones and very fine- to fine-grained sandstones with rip-up clasts and soft sediment deformation.|
28203|Angepena Formation|73227|6|Mentioned|p36|||Adelaide Superbasin. May have been a lateral fluid conduit.||||||
28203|Angepena Formation|73234|6|Mentioned|p6|||Deposited in shallow marine to tidal flat environments.|||||Silty to sandy.|
28203|Angepena Formation|73236|4|Described|p35-39, p47|Cryogenian|Cryogenian|Early Marinoan redbeds. Marine/mud-flat sedimentary rocks. Occurs only as glacial erratics in Hallett Cove map area. Deposition under conditions of post-rift thermal subsidence.||Upalinna Subgroup, Umberatana Group, Heysen Supergroup||Underlain by Brighton Limestone (Nepouie Subgroup). Overlain by Wilmington Formation.|Reddish grey sandy siltstone with ripple-marked, dark red shale partings.|
28203|Angepena Formation|74367|6|Mentioned|p19||||618+/- 136 Ma Rb-Sr (Webb et al., 1983)|||||
81784|Angle Dam Dacite|72237|4|Described|p28-32|Mesoproterozoic|Mesoproterozoic|Geological province: Gawler Craton. Of Roopena Basin.||Unit of Gawler Range Volcanics.||Basal unit of the Gawler Range Volcanics. Overlain by lower Fresh Well Formation.|Porphyritic volcanics.|
81784|Angle Dam Dacite|73162|4|Described|p447-448, p450-455, p457,p458, p460|Mesoproterozoic|Mesoproterozoic|Roopena Basin. Thickness of 14-43 m from drill cores. North-south trending linear body 300 m wide by 900 m wide. Oldest part of the Gawler Range Volcanics succession at Roopena.||lower Gawler Range Volcanics||Overlies the Moonabie Formation. Underlies the Fresh Well Formation and Roopena Basalt.|Evenly porphyritic lava; phenocrysts of euhedral to subhedral feldspar, quartz and biotite in a fine-grained groundmass.|
41897|Anthony Member|61234|4|Described|p6, p7 Fig 4.|Late Eocene|Late Eocene|Of the Pidinga Formation. Overlies Maralinga Member. Marginal marine - fluvial carbonaceous clastics. Geological Province: Eucla Basin.||||||22-JAN-15
41897|Anthony Member|61856|5|Briefly described|p300 Fig.2, p311-315|Late Eocene|Late Eocene|New name, formerly the upper Pidinga Formation. To include all Late Eocene estuarine-fluvial clastics and lignites in the coastal zones of the eastern Eucla Basin.||Of the Pidinga Formation||Is overlain by Khasta Formation.||
41897|Anthony Member|64646|6|Mentioned|p23 Fig. 3|Oligocene|Eocene|Of Pidinga Formation. Geological Province: Gawler Craton.||||||
41897|Anthony Member|67462|5|Briefly described|Map legend.|Eocene|Eocene|Eucla Basin.||Unit in Pidinga Formation.||Overlies Maralinga Member.||
41897|Anthony Member|68715|6|Mentioned|p30 Fig.5|Priabonian|Bartonian|SW and NW Gawler Craton, Eucla Basin.||Pidinga Formation.||||07-APR-17
41897|Anthony Member|69598|6|Mentioned|p9|Middle Eocene|Middle Eocene|||||||
72293|Antro Suite|62514|5|Briefly described|p748 Fig. 3|Mesoproterozoic|Mesoproterozoic|I-type granitoids. Age: 1.64-1.63Ga. Geological Province: Olary Domain/Curnamona Province||||||16-SEP-09
34536|Apamurra Formation|22746|5|Briefly described|Fig.3 p515|Early Cambrian|Early Cambrian|||||||
34536|Apamurra Formation|22922|5|Briefly described|34|||||||||
34536|Apamurra Formation|23282|2|Defined|p77||Early Cambrian|Age: Early Cambrian 518 - 516Ma. of Marla Group, Officer Basin. Originally defined as the Apamurra Member of Mt Johns Conglomerate Benbow (1982). Now raised to formation and Mt Johns C demoted to member of Apamurra Fm.||||||
34536|Apamurra Formation|23288|6|Mentioned|Fig.5||Early Cambrian|||||||
34536|Apamurra Formation|23524|5|Briefly described|p221 Fig. 3|Early Cambrian|Early Cambrian|||||||
34536|Apamurra Formation|24112|5|Briefly described|p254 Fig.2|Early Cambrian|Early Cambrian|Geological Province: Officer Basin||||||
34536|Apamurra Formation|44133|5|Briefly described|p38-39, 4 Fig. 7.2|Middle Paleozoic|Early Paleozoic|Geological Province: Eastern Officer Basin. Maximum Thickness: 70m.||||||07-NOV-08
34536|Apamurra Formation|60565|5|Briefly described|p20 Fig. 3b|||Overlain by the Trainor Hill Sandstone. Overlies the Arcoeillinna Sandstone.||||||16-JUN-05
34536|Apamurra Formation|60953|5|Briefly described|Map Legend|Cambrian|Cambrian|Shallow marine to tidal flat calcareous siltstone, sandstone, minor limestone, alluvial fan conglomerate and sandstone.||||||
34536|Apamurra Formation|61108|5|Briefly described|map legend|Cambrian|Cambrian|Shallow marine to tidal flat calcareous siltstone, sandstone, minor limestone, alluvial fan conglomerate and sandstone.||||||
34536|Apamurra Formation|62570|5|Briefly described|p580 Figs. 2 and 3|Middle Cambrian|Middle Cambrian|Of the Marla Group. Geological Province: Officer Basin. Calcareous siltstones.||||||10-AUG-07
34536|Apamurra Formation|65313|6|Mentioned|p578 Fig. 6|Middle Cambrian|Middle Cambrian|Officer Basin.||Of Marla Group.||Underlies Trainor Hill Sandstone, overlies Observatory Hill Formation.||26-MAR-12
34536|Apamurra Formation|67120|5|Briefly described|Map legend|Cambrian|Cambrian|||Of Marla Group|||Siltstone, calcareous; sandstone, fine-grained; minor limestone and cross-bedded sandstone.|12-JAN-16
34536|Apamurra Formation|67536|6|Mentioned|Map Legend|||One of several Formations mapped collectively as Em5.|||||Mostly non-marine sandstone, siltstone, claystone and minor dolomite, limestone, chert and conglomerate.|
34536|Apamurra Formation|70336|5|Briefly described|Map legend|Cambrian|Cambrian|||Of Marla Group.|Includes Mount Johns Conglomerate Member.||Calcareous siltstone; fine-grained sandstone; minor limestone and cross-bedded sandstone.|12-JAN-16
34536|Apamurra Formation|70839|5|Briefly described|p342-343|Early Cambrian|Early Cambrian|Of East Officer Basin. Late early Cambrian age based on stratigraphic position within biostratigraphically dated succession and revised radiometric age of overlying Table Hill Volcanics (Morton and Drexel, 1997; Jourdan et al., 2014).||||Overlain by Table Hill Volcanics.||
34536|Apamurra Formation|71618|6|Mentioned|p130|||Of Officer Basin.||||||
34536|Apamurra Formation|72478|6|Mentioned|p8, p11|Early Cambrian|Early Cambrian|Officer Basin. See also p51 [of the document].|c. 518-516 Ma|Marla Group|Includes Mount Johns Conglomerate Member.|||25-MAR-21
34536|Apamurra Formation|73099|5|Briefly described|Map legend.|Middle Cambrian|Early Cambrian|Officer Basin.||Marla Group.||Overlies Arcoeillinna Sandstone. Is overlain by Trainor Hill Sandstone.|Medium-brown to red-brown, laminated to thin-bedded, micaceous siltstone, partly calcareous and dolomitic; interbeds of very fine- to medium-grained sandstone in upper part of Formation.|
34536|Apamurra Formation|73392|6|Mentioned|p3||||||||Sampled from core of Birksgate 1 well.|
34654|Arbury Park Sandstone Member|22869|2|Defined|P38, P45, Fig3||Neoproterozoic|New name, correlated with Rhynie Sandstone, Top Mount Sandstone and Humanity Seat Formation, overlying unit is Carey Gully Sandstone Member||||||
34654|Arbury Park Sandstone Member|22889|6|Mentioned|Table 1 on p32|Adelaidean|Adelaidean|Parent - Aldgate Sandstone of the Emeroo Subgroup.||||||
24164|Arcoeillinna Sandstone|22922|5|Briefly described|34|||Parent Marla Group||||||
24164|Arcoeillinna Sandstone|23282|2|Defined|p76||Early Cambrian|Age: Early Cambrian 520 - 518Ma. of Marla Group, Officer Basin. of Benbow (1982). May be equivalent to 'Wirrildar beds' in Central OB, interpreted equiv in Arrowie Basin is upper part of Billy Creek Formation.||||||02-MAR-10
24164|Arcoeillinna Sandstone|23288|6|Mentioned|Fig.5||Early Cambrian|||||||
24164|Arcoeillinna Sandstone|23524|5|Briefly described|p221 Fig. 3|Early Cambrian|Early Cambrian|||||||
24164|Arcoeillinna Sandstone|24112|5|Briefly described|p254 Fig.2|Early Cambrian|Early Cambrian|Of the Marla Group. Geological Province: Officer Basin||||||
24164|Arcoeillinna Sandstone|38329|2|Defined|p201|Cambrian|Cambrian|||||||
24164|Arcoeillinna Sandstone|40945|6|Mentioned|Fig.3|||||||||
24164|Arcoeillinna Sandstone|43052|5|Briefly described|Fig.2.10|||||||||
24164|Arcoeillinna Sandstone|43053|5|Briefly described|Map Legend|Cambrian|Cambrian|Of the Marla Group. Fluviolacustrine and aeolian lithic sandstone.||||||25-MAY-05
24164|Arcoeillinna Sandstone|43258|5|Briefly described|Map Legend||Cambrian|||||||
24164|Arcoeillinna Sandstone|43298|5|Briefly described|Map Legend||Cambrian|||||||
24164|Arcoeillinna Sandstone|43690|6|Mentioned|Fig.2,p157||Cambrian|||||||
24164|Arcoeillinna Sandstone|43732|6|Mentioned|Fig.4,p5||Early Cambrian|||||||
24164|Arcoeillinna Sandstone|43743|6|Mentioned|Fig.2,p33||Early Cambrian|||||||
24164|Arcoeillinna Sandstone|44109|5|Briefly described|p22 Fig. 19|Cambrian|Cambrian|Of the Marla Group. Geological Province: central Officer Basin.||||||
24164|Arcoeillinna Sandstone|44133|5|Briefly described|p37-38, 4 Fig. 7.2|Middle Paleozoic|Early Paleozoic|Geological Province: Eastern Officer Basin. Of the Marla Group. Overlies Observatory Hill Formation, Wallatinna Formation (disc). ||||||07-NOV-08
24164|Arcoeillinna Sandstone|60953|5|Briefly described|Map Legend|Cambrian|Cambrian|Fluviolacustrine and aeolian lithic sandstone.||||||
24164|Arcoeillinna Sandstone|61108|5|Briefly described|map legend|Cambrian|Cambrian|Fluviolacustrine and aeolian lithic sandstone.||||||
24164|Arcoeillinna Sandstone|62570|5|Briefly described|p580 Figs. 2 and 3|Middle Cambrian|Middle Cambrian|Of the Marla Group. Geological Province: Officer Basin. Arkosic unit.||||||10-AUG-07
24164|Arcoeillinna Sandstone|67120|5|Briefly described|Map legend|Cambrian|Cambrian|||Marla Group|||Sandstone, red-brown, very fine to medium-grained, moderately well sorted and immature. Interbedded with claystone and siltstone. Also minor pebbly horizons. Clasts of claystone.|
24164|Arcoeillinna Sandstone|67536|6|Mentioned|Map Legend|||One of several Formations mapped collectively as Em5.|||||Mostly non-marine sandstone, siltstone, claystone and minor dolomite, limestone, chert and conglomerate.|
24164|Arcoeillinna Sandstone|70336|5|Briefly described|Map legend|Cambrian|Cambrian|||Marla Group.|||Red-brown, very fine- to medium-grained, moderately well-sorted and immature sandstone; interbedded with claystone and siltstone. Minor pebbly horizons; clasts of claystone.|
24164|Arcoeillinna Sandstone|71342|6|Mentioned|Ch9 p3, Ch9 p9, Ch9 p11-p12, Ch9 p15|Cambrian|Cambrian|Thermal history briefly described (Ch9 p3).||||||
24164|Arcoeillinna Sandstone|72478|5|Briefly described|p8|Early Cambrian|Early Cambrian|Officer Basin. See also Arcoelinna Sandstone p11, p51 [of the document] p8 of App 1.|c. 520-518Ma|Marla Group||Overlies Observatory Hill Formation. Overlain by Apamurra Formation.||24-MAR-21
24164|Arcoeillinna Sandstone|73099|5|Briefly described|Map legend.|Middle Cambrian|Early Cambrian|Officer Basin.||Marla Group.||Overlies Observatory Hill Formation. Is overlain by Apamurra Formation.|Off-white to red-brown, thin- to thick-bedded, very fine- to medium-grained, partly micaceous quartz sandstone, interbedded with red-brown, micaceous claystone and siltstone.|
24164|Arcoeillinna Sandstone|73392|6|Mentioned|p3||||||||Sampled from core of Birksgate 1 well.|
32304|Argonaut Member|12796|5|Briefly described|p456 Fig. 2|Santonian|Coniacian|Represents a thick lenticular sequence of interbedded sandstones and shales at the base of the Mount Salt Formation (Sherbrook Group). Geological Province: Otway Basin/Gambier Embayment.||||||
32304|Argonaut Member|24314|5|Briefly described|p 61 Fig.2|Santonian|Santonian|Geological Province: Otway Basin. Of the Sherbrook Group.||||||
32304|Argonaut Member|61547|6|Mentioned|p461 Fig.2, p462. |Santonian|Santonian|||||||
32304|Argonaut Member|63431|5|Briefly described|p677 Fig. 2|||Parent unit is unclear but ultimately this member is part of the Sherbrook Group.||||||07-FEB-11
82223|Aristarchus Metaperidotite|73230|1|Redefined|p6, p9-10, p12-14, p15-16|Siderian[?]|Siderian|Redefined name [see appendix and ASUD for definition]; formerly Aristarchus Peridotite. Gawler Craton. Domain: Christie and Wilgena. Only weakly foliated. Contains elevated nickel contents with magmatic nickel mineralisation occurring as disseminated, interstitial sulfides including pentlandite and violarite. Known from lithostratigraphic correlations to be younger than the Burden Metagabbro. Named after Aristarchus Rise on the TARCOOLA mapsheet. Previously known as Aristarchus Peridotite; previous definition also included the newly named Burden Metagabbro. Type locality: drillhole Aristarchus 1 (3239), interval 99.5-106.1 m. Reference drillhole: DMDD-002 (234168), interval 307.44-307.89 m. Occurs in drillholes near Aristarchus Paddock in the southern Christie Domain. Thickness: Up to 7 m, but typically 0.2-0.4 m thick in type drillhole. Age constrained by crosscutting relationship with Aurora Tank Suite. Potential correlative of [Skuse] Hill Metapyroxenite.|Younger than c. 2475Ma (magmatic)|Mulgathing Complex||Intrudes Aurora Tank Suite, Burden Metagabbro and Christie Gneiss.|Pargasite-tremolite-serpentine-olivine amphibolite dykes interpreted as metaperidotite (lherzolite) also containing chromite, ilmenite and magnetite.|
29894|Armchair Granite|43052|5|Briefly described|Table 4.8|||||||||
29894|Armchair Granite|50605|5|Briefly described|p10.2|||Of the Babbage Supersuite. Geological Province: Gawler Craton & Curnamona Province.||||||
29894|Armchair Granite|70384|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Age uncertain.|||||Granite, brick-red, equigranular; microcline, plagioclase, magnetite, minor fluorite, brannerite and biotite.|
26354|Aroona Creek Limestone|22766|5|Briefly described|Fig.2 p561, p562|Early Cambrian|Early Cambrian|||||||
26354|Aroona Creek Limestone|23818|5|Briefly described|p87 Fig.33|Cambrian|Cambrian|||||||
26354|Aroona Creek Limestone|23981|5|Briefly described|p8-9 Fig. 4|Toyonian|Toyonian|Overlies Billy Creek Formation. Geological Province: Arrowie Basin.||||||12-JUL-06
26354|Aroona Creek Limestone|24176|5|Briefly described|p17|Middle Cambrian|Middle Cambrian|Equivalent to Wirrealpa Limestone (BALCANOONA).   Referred to as Wirrealpa Limestone-Aroona Creek Limestone (undifferentiated) in Table1 (p23).||||||
26354|Aroona Creek Limestone|24465|5|Briefly described|p345 Fig.2|Middle Cambrian|Early Cambrian|Geological Province: Arrowie Basin.||||||19-JAN-05
26354|Aroona Creek Limestone|30051|6|Mentioned|Fig.4|||||||||
26354|Aroona Creek Limestone|30176|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
26354|Aroona Creek Limestone|30801|6|Mentioned|p5|||Middle Cambrian. See also P6. Table.||||||03-MAY-13
26354|Aroona Creek Limestone|30807|6|Mentioned|p102|||Suggested map symbol||||||
26354|Aroona Creek Limestone|32343|6|Mentioned|Table 1|||||||||
26354|Aroona Creek Limestone|33972|4|Described|p15|||Mention P13||||||
26354|Aroona Creek Limestone|34268|6|Mentioned|p241|||Cambrian||||||
26354|Aroona Creek Limestone|34612|6|Mentioned|Fig.33|||Cambrian||||||
26354|Aroona Creek Limestone|34766|6|Mentioned|p58|||||||||
26354|Aroona Creek Limestone|35255|6|Mentioned|Fig.8|||||||||
26354|Aroona Creek Limestone|35543|6|Mentioned|Fig.1|||Regional bedrock geology.||||||
26354|Aroona Creek Limestone|35835|6|Mentioned|p207|||||||||
26354|Aroona Creek Limestone|35954|6|Mentioned|p1230|||See also Fig.2.||||||
26354|Aroona Creek Limestone|36081|6|Mentioned|Fig.1|||||||||
26354|Aroona Creek Limestone|36083|5|Briefly described|p473|||||||||
26354|Aroona Creek Limestone|36198|6|Mentioned|p249|||See also Fig.I.2||||||
26354|Aroona Creek Limestone|36495|6|Mentioned|Fig.12|||||||||
26354|Aroona Creek Limestone|37113|6|Mentioned|Fig.1|||||||||
26354|Aroona Creek Limestone|37802|6|Mentioned|Fig.2|||||||||
26354|Aroona Creek Limestone|38068|6|Mentioned|p69|||||||||
26354|Aroona Creek Limestone|40852|6|Mentioned|p33|||||||||
26354|Aroona Creek Limestone|40856|6|Mentioned|Fig.23.6|||||||||
26354|Aroona Creek Limestone|41457|6|Mentioned|Fig.2|||||||||
26354|Aroona Creek Limestone|41526|6|Mentioned|p60|||||||||
26354|Aroona Creek Limestone|42141|6|Mentioned|Table 2 P571|||||||||
26354|Aroona Creek Limestone|42222|6|Mentioned|Table 1 P5|||||||||
26354|Aroona Creek Limestone|42225|6|Mentioned|p223|||||||||
26354|Aroona Creek Limestone|42269|6|Mentioned|p337|||||||||
26354|Aroona Creek Limestone|42440|6|Mentioned|Fig.2 P602|||||||||
26354|Aroona Creek Limestone|43011|6|Mentioned|Table 2,p12|||||||||
26354|Aroona Creek Limestone|44133|5|Briefly described|p4 Fig. 7.2, 17, 27-28|Early Cambrian|Early Cambrian|Geological Province: Arrowie Basin. Maximum Thickness: 70m.||||||
26354|Aroona Creek Limestone|60889|6|Mentioned|p247 Fig.4|Early Cambrian|Early Cambrian|||||||
26354|Aroona Creek Limestone|60990|6|Mentioned|p83 Fig.2|Toyonian|Toyonian|Flinders Ranges.||||||
26354|Aroona Creek Limestone|63447|6|Mentioned|p963 Fig.2|Early Cambrian|Early Cambrian|Arrowie Basin||||Overlies Billy Creek Formation. Wirrealpa Limestone shown as lateral equivalent.||
26354|Aroona Creek Limestone|63569|6|Mentioned|p117 Fig.1|Early Cambrian|Early Cambrian|Arrowie Basin.||||Overlies Billy Creek Formation. Is overlain by Moodlatana Formation.||
26354|Aroona Creek Limestone|64829|5|Briefly described|p1084 Fig. 1|Cambrian|Cambrian|||||||07-FEB-11
26354|Aroona Creek Limestone|65313|6|Mentioned|p576 Fig. 5|Cambrian|Cambrian|||||||
26354|Aroona Creek Limestone|65625|5|Briefly described|p103 Fig.2|Middle Cambrian|Middle Cambrian|Mount Scott Range area.||||||13-APR-11
26354|Aroona Creek Limestone|65686|6|Mentioned|p413, 415|Early Cambrian|Early Cambrian|Arrowie Basin.||||||07-MAY-12
26354|Aroona Creek Limestone|65892|5|Briefly described|p9 Fig.4, p41, p45.|Early Cambrian|Early Cambrian|East Arrowie Basin. Basal 15m contains Redlichia guizhouensis.||||Conformably overlies Eregunda Sandstone Member. Correlative of Wirrealpa Limestone.|Bottom few metres are well-bedded, grey, locally stromatolitic, peloidal, oolitic and fenestral, limestone.|
26354|Aroona Creek Limestone|65925|6|Mentioned|p14 Fig.2.2.|Early Cambrian|Early Cambrian|||||||
26354|Aroona Creek Limestone|68735|5|Briefly described|p233 Fig.2, p234, p235 Fig.3|Early Cambrian|Early Cambrian|Arrowie Basin. Equivalent to the Wirrealpa Limestone of the Mount Scott Range area.||||Overlies Billy Creek Formation.||10-APR-17
26354|Aroona Creek Limestone|68993|6|Mentioned|p544 Fig.1|Early Cambrian|Early Cambrian|Arrowie Basin.||||||
26354|Aroona Creek Limestone|71241|14|Not recorded|p14|Middle Cambrian|Middle Cambrian|In use for Middle Cambrian limestone near Mount Scott.||||||
23342|Arrabury Formation|13497|4|Described|iv, viii, xii, p69 fig 6.1, p102|Early Triassic|Late Permian|Cooper Basin. Defined by Powis (1989) as the basal unit of the Nappamerri Group and a type section was deisgnated also. Maximum thickness of 400m in the Patchawarra Trough. Seals the Toolachee Formation and forms a regional seal over all the Permian formations of the basin. Wireline log results are discussed. See also p104-p106, p108, p110, p112, p114, p119, p125, p127, p165-p166, p169-p174, p179.||Nappamerri Group|Includes the Callamurra Member, Paning Member and the Wimma Sandstone Member.|Conformably overlies the Toolachee Formation. Unconformably overlies the Innamincka Formation. Conformably overlain by the Tinchoo Formation. Disconformably overlain by the Hutton Sandstone.|Dark to pale grey siltstone and mudstone beds with interbedded pale-grey and cross-bedded sandstones.|
23342|Arrabury Formation|13516|5|Briefly described|p171 fig 12|Early Triassic||In Eromanga Basin.|||Includes Callamurra Member, Wimma Sandstone Mmember|||
23342|Arrabury Formation|22839|6|Mentioned|P33|Early Triassic|Late Permian|||||||
23342|Arrabury Formation|22883|6|Mentioned|P29|Early Triassic|Late Permian|Underlying unit is Toolachee Formation||||||
23342|Arrabury Formation|23154|5|Briefly described|Map Legend|Triassic|Permian|Geological Province - Cooper Basin. Parent - Nappamerri Group.||||||16-FEB-10
23342|Arrabury Formation|23155|4|Described|p23 & Fig 13 on p24|Mesozoic|Mesozoic|Contains a sparse unusually oxidised pollen assemblage indicative of a Late Permian to Early Triassic age.||||||
23342|Arrabury Formation|23375|4|Described|Fig2 p265,283|Spathian|Dzhulfian|In the Cooper Basin.||||||17-JAN-08
23342|Arrabury Formation|24210|5|Briefly described|p133 Fig. 2|Middle Triassic|Late Permian|Of the Nappamerri Group. Includes the Callamurra and Paning Members and the Wimma Sandstone Members. Geological Province: Cooper Basin.||||||16-FEB-10
23342|Arrabury Formation|42008|2|Defined|p269|Anisian|Tatarian|See also Fig.2, Fig.3||||||
23342|Arrabury Formation|42085|6|Mentioned|Fig.2 P374|||||||||
23342|Arrabury Formation|43052|5|Briefly described|Table 2.1|||||||||
23342|Arrabury Formation|44133|4|Described|p65 Fig. 8.3, 85|Triassic|Permain|Of the Nappamerri Group. Geological Province: Cooper Basin. Includes: Callamurra Member, Paning Member, Wimma Sandstone Member. Overlies: Toolachee Formation .||||||17-JAN-08
23342|Arrabury Formation|60386|6|Mentioned|p299|Early Triassic|Early Triassic|Cooper/Eromanga Basin. Non-marine.||||||
23342|Arrabury Formation|60717|5|Briefly described|p40 Fig. 2|Anisian|Tatarian|Of Nappamerri Group. Contains Callamurra and Paning Members, and Wimma Sandstone Member. Overlies Toolachee Formation; overlain by Tinchoo Formation. Combined thickness = 375m. Geological Province: Cooper Basin.||||||31-JAN-08
23342|Arrabury Formation|61613|5|Briefly described|p282 Fig. 2|Triassic|Late Permian|Of Nappamerri Group. Includes Callamurra, Paning and Wimma Sandstone Members. Overlain by Tinchoo Formation. Geological Province: Cooper and Simpson Basins.||||||07-FEB-11
23342|Arrabury Formation|61614|6|Mentioned|p290 Fig. 2|Middle Triassic|Late Permian|Of Nappamerri Group. Geological Province: Cooper Basin.||||||17-MAR-09
23342|Arrabury Formation|61615|6|Mentioned|p302 Fig. 2|Middle Triassic|Late Permian|Of Nappamerri Group. Geological Province: Cooper Basin.||||||07-FEB-11
23342|Arrabury Formation|61616|6|Mentioned|p330 Fig. 2|Early Triassic|Late Permian|Of Nappamerri Group. Includes Wimma Sandstone, Paning and Callamurra Members. Geological Province: Cooper Basin.||||||
23342|Arrabury Formation|62537|6|Mentioned|p191 Fig.2. |Middle Triassic|Early Triassic|Cooper Basin.||Unit in Nappamerri Group.|Includes Wimma Sandstone, Callamurra and Paring Members.|Overlies Toolachee Formation. Is overlain by Tinchoo Formation.||
23342|Arrabury Formation|62730|5|Briefly described|p352 Fig. 1|Late Triassic|Late Permian|Of the Nappamerri Group. Includes the Callamurra Member. Geological Province: Eromanga Basin.||||||21-APR-08
23342|Arrabury Formation|63978|2|Defined|p7, p19, Fig. 3|Early Triassic|Late Permian|Basal unit of Nappamerri Group. Includes the Wimma Sandstone, Paning and Callamurra Members. Conformably overlies Toolachee Fm. Unconformably overlies Innamincka Fm. (Warburton Basin). Max. thick: 412m. In Cooper Basin. Detailed lithology included.||||||07-FEB-11
23342|Arrabury Formation|64048|5|Briefly described|p64 Tb. 2|Early Traissic|Late Permian|Basal unit of the Nappamerri Group. Contains the Callamurra, Paning and Wimma Sandstone Members. Unconformably overlain by Tinchoo Formation.  Geological Province:Cooper Basin.||||||07-FEB-11
23342|Arrabury Formation|64197|6|Mentioned|p625 Fig.1c|Middle Triassic|Late Permian|||Nappamerri Group|Includes Callamurra, Paning, and Wimma [Sandstone], Members.|Overlies Toolachee Formation. Is overlain by Tinchoo Formation.||
23342|Arrabury Formation|64665|5|Briefly described|p53 Fig.2.|Middle Triassic|Early Triassic|Cooper Basin.|||Includes Callamurra, Paning, and Wimma Sandstone, Members.|Overlies Toolachee Formation. Is overlain by Tinchoo Formation.||
23342|Arrabury Formation|65238|5|Briefly described|p9|Triassic|Triassic|Geological province: Cooper Basin. Red bed succession in sedimentary continuum with the underlying Toolachee Formation. Unconformably underlies Tinchoo Formation.||||||17-FEB-10
23342|Arrabury Formation|65489|5|Briefly described|p15, p48-49, p55, p96, p131-132|Early Triassic|Early Triassic|Cooper Basin. Gas and oil reservoir accounting for 1% each of the Basin's production. Regional seal. Shown as Tatarian to Anisian on p48.||Unit in Nappamerri Group.|Includes Callamurra, Paning, and Wimma Sandstone, Members.|Overlies Toolachee Formation (Gidgealpa Group). Is overlain by Tinchoo Formation. Probably equivalent to Walkandi Formation.||
23342|Arrabury Formation|65925|5|Briefly described|Appendix 2.||||||||Red beds, sandstone, siltstone, mudstone carbonaceous in part. Fluvial, fluvio-lacustrine.|
23342|Arrabury Formation|67402|6|Mentioned|p90, p90 fig CPR4, p91, p92|||||Nappamerri Group|Includes the Callamurra Member, Paning Member and the Wimma Sandstone Member.|Unconformably overlain by the Tinchoo Formation. Overlies the Gidgealpa Group.||
23342|Arrabury Formation|68731|4|Described|p200 Fig 3.110, pp208-211|Anisian|Lopingian|Cooper Basin. ~ 420-200 m thick. Deposition was on a vegetated flood plain with ephemeral lakes in lowland areas and pedogenesis in exposed areas. Palynological dating indicates a late Lopingian-early Anisian age (Gray and McKellar 2002).||Basal unit of the Nappamerri Group.|Includes the Callamurra Member, Paning Member, and the Wimma Sandstone Member.|Conformably underlain by the Toolachee Formation. Unconformably overlain by the Tinchoo Formation.|Comprises interbedded sandstone, siltstone and mudstone with some redbed characteristics. Siderite occurs as speckles, diffuse layers and as patchy cement.|02-JUL-14
23342|Arrabury Formation|69454|5|Briefly described|p38:4|Anisian|Changhsingian|Cooper Basin. Appears as Arrabury Sandstone on 38:8.||Nappamerri Group.||Correlated with Walkandi Formation (Pedirka Basin).||12-JUL-16
23342|Arrabury Formation|69673|6|Mentioned|p153 fig 125|||||Nappamerri Group||Overlain by Tinchoo Formation, overlies Toolachie Formation||
23342|Arrabury Formation|69728|6|Mentioned|p285|||Cooper Basin.||Nappamerri Group.||||
23342|Arrabury Formation|69797|5|Briefly described|p17 Fig.2|Middle Triassic|Late Permian|Age: Tatarian - Anisian (approximated from figure). Geol. Prov: Cooper Basin.||Nappamerri Group|Wimma Sandstone Member, Paning Member, Callamurra Member|||
23342|Arrabury Formation|69946|5|Briefly described|p9, p36, p54, p68|Early Triassic|Permian|Cooper Basin. Tatarian to Anisian.||Unit in Nappamerri Group.|Includes Paning, Wimma Sandstone and Callamurra Members.|Conformably overlies Toolachee Formation. Is overlain conformably by Tinchoo Formation.||
23342|Arrabury Formation|69947|5|Briefly described|p13 Fig.7.2|Early Triassic|Permian|Cooper Basin.||Nappamerri Group.|Callamurra, Paning, Wimma Sandstone, Members.|||
23342|Arrabury Formation|69982|5|Briefly described|p44, p62, p68|Triassic|Triassic|Hydrocarbon shows from the Warburton Basin rocks have been incorrectly assigned to this unit (and others). Brief thin section descriptions.|||||Redbeds.|
23342|Arrabury Formation|70317|5|Briefly described|p33|Middle Triassic|Late Permian|Cooper Basin. Lacustrine, flood plain depositional environment.||Nappamerri Group.|Callamurra, Paning, Wimma Sandstone, Members.|Overlies Toolachee Formation. Is overlain by Callamurra Member (Arrabury Formation).||
23342|Arrabury Formation|70823|4|Described|iv, p40, p70,|Olenekian|Late Permian|Cooper Basin. Deposited in braided fluvial, floodplain or lacustrine environments. Distribution, outcrop and palynological characteristics are discussed briefly. This unit is generally 200 to 350m thick in the Nappamerri Trough and between 380 to 390m thick in the Arrabury Trough. Hosts a commercial reservoir. See also p75-p76, p78-p79, p81-p82.||Nappamerri Group|Includes the Callamurra Member, Paning Member and the Wimma Sandstone Member.|Conformably overlies the Toolachee Formation. Unconformably overlies the Warburton Formation.  Conformably overlain by the Tinchoo Formation.|Basal mudstone and siltstone with thin fine to medium-grained quartzose sandstone interbeds.|
23342|Arrabury Formation|70824|4|Described|p7-p9, p104|Olenekian|Induan|Cooper Basin. Up to 400m thick.||Nappamerri Group|Includes the Callamurra Member, Paning Member and the Wimma Sandstone Member.|Overlies the Toolachee Formation. Overlain by the Tinchoo Formation.|Basal mudstone and siltstone with thin fine to medium-grained quartzose sandstone interbeds overlain by sandstone with minor siltstone interbeds.|
23342|Arrabury Formation|70946|5|Briefly described|p1089|Middle Triassic|Permian|Cooper Basin.||Nappamerri Group.|Callamurra, Paning, Wimma Sandstone, Members.|Overlies the Toolachee Formation. Overlain by the Tinchoo Formation.||08-OCT-18
23342|Arrabury Formation|71265|5|Briefly described|p589|Induan|Olenekian|Cooper Basin.||Nappamerri Group.|Callamurra, Paning Members.|Overlies Toolachee Formation.||
23342|Arrabury Formation|71342|5|Briefly described|Ch5 p9, Ch5 p31, Ch5 p36|Anisian|Tatarian|Cooper Basin. Palynological zone is given in fig 5.3 Ch5 p36. Deposited in a braided fluvial, floodplain or lacustrine environment. See also Ch5 p54, Ch5 p67, Ch7 p13.||Nappamerri Group|Includes the Paning, Wimma Sandstone and the Callamurra Members.|Conformably overlies the Toolachee Formation.||
23342|Arrabury Formation|71701|4|Described|p155|Olenekian|Induan|Cooper Basin.||Nappamerri Group|Includes the Paning and Callamurra members.|Overlies the Toolachee Formation.||
23342|Arrabury Formation|72297|5|Briefly described|p742|||Cooper Basin.|||Callamurra Member.|||
23342|Arrabury Formation|73251|6|Mentioned|p62|Middle Triassic|Permian|Cooper Basin. Braided fluvial channel belt, floodplain, lacustrine, and moderately sinuous fluvial channel depositional environments.||Nappamerri Group|Wimma Sandstone Member, Paning Member, Callamurra Member|Underlain by Toolachee Formation (Gidgealpa Group). Overlain by Tinchoo Formation.||
29921|Arthurton Granite|22430|6|Mentioned|p2||Proterozoic|||||||
29921|Arthurton Granite|22629|5|Briefly described|fig2, p,152,158|Calymmian|Calymmian|1600-1575Ma||||||
29921|Arthurton Granite|23719|5|Briefly described|p17 table 4|Calymmian|Calymmian|Age: 1582+/-7 Ma (U-Pb zircon). Geological Province: Gawler Craton.||||||
29921|Arthurton Granite|23803|5|Briefly described|p29 Fig. 2|Paleoproterozoic|Paleoproterozoic|Age: 1770-1730Ma. Geological Province: Gawler Craton.||||||07-NOV-08
29921|Arthurton Granite|24197|5|Briefly described|p30|||Of the Hiltaba Suite (Roxby Downs type). Geological Province: Gawler Craton.||||||07-FEB-11
29921|Arthurton Granite|24360|6|Mentioned|p53|||Geological Province: Yorke Peninsula, Gawler Craton||||||
29921|Arthurton Granite|24475|5|Briefly described|p46|Mesoproterozoic|Mesoproterozoic|Of Hiltaba Suite.||||||
29921|Arthurton Granite|24585|5|Briefly described|p32|Calymmian|Calymmian|Intrudes the Wallaroo Group. Age: ~1582Ma.||||||23-DEC-09
29921|Arthurton Granite|43052|5|Briefly described|Table 5.6|||||||||
29921|Arthurton Granite|43053|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of Hiltaba Suite. Anorogenic granitoids. Geological Province: Gawler Craton.||||||
29921|Arthurton Granite|43258|5|Briefly described|Map Legend||Mesoproterozoic|||||||
29921|Arthurton Granite|43298|6|Mentioned|Map Legend||Mesoproterozoic|||||||
29921|Arthurton Granite|50605|5|Briefly described|p8.1|Mesoproterozoic|Mesoproterozoic|Of the Roxby Downs Suite (Hiltaba Supersuite). Age: 1583 +/- 3Ma (U-Pb). Geological Province: Gawler Craton & Curnamona Province.||||||
29921|Arthurton Granite|60958|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of the Hiltaba Suite. Pink, coarse-grained, A Type adamellite. Undeformed to foliated. Age: 1582 +/- 7Ma. Geological Province: Gawler Craton.||||||14-APR-05
29921|Arthurton Granite|61121|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Hiltaba Suite. Pink, coarse-grained, A-type adamellite with quartz, microcline, plagioclase, mica, sphene, magnetite and chlorite; undeformed to foliated; often pegmatitic or miarolitic. Age: 1582+/-7Ma. Geological Province: Gawler Craton.||||||02-JUN-05
29921|Arthurton Granite|63398|5|Briefly described|p663, p666|Mesoproterozoic|Mesoproterozoic|Of Hiltaba Suite. Surrounds/intrudes Curramulka Gabbronorite; also intruded Wallaroo Group. Age: 1582+/-7Ma (U-Pb). Geol.Prov: Gawler Craton. Comprises pink, coarse-grained adamellite or monzogranite with minor granodiorite and rare tonalite-trondhjemite.||||||10-DEC-07
29921|Arthurton Granite|65375|4|Described|p7, p13, p21.|Mesoproterozoic|Mesoproterozoic|Underlies much of northern and central Yorke Peninsula. Equivalent to Tickera Granite in the north. Has a close relationship with Curramulka Gabbronorite.|1582 +/- 7 Ma.|||Intrudes Wallaroo Group.|Pink, coarse-grained adamellite consisting mainly of quartz, microcline, plagioclase, mica, sphene, tourmaline, magnetite and chlorite; usually pegmatitic.|
29921|Arthurton Granite|65376|5|Briefly described|p112.|||A-type granite.|1582 +/- 7 Ma.|Unit in Hiltaba Suite.|||Granite, adamellite, quartz-monzonite.|
29921|Arthurton Granite|65390|5|Briefly described|p18, p23 Fig.3, p26 Tb. 1|Calymmian|Calymmian|Olympic Domain, Gawler Craton. Equivalent of Moonta Adamellite, which has a U-Pb zircon age of 1583 +/- 7 Ma.||||||
29921|Arthurton Granite|66302|6|Mentioned|p47|Calymmian|Calymmian|Olympic Domain, Gawler Craton.|1582 +/-7 (Creaser and Cooper, 1993)|Hiltaba Suite||Intrudes the Wallaroo Group.||
29921|Arthurton Granite|67345|6|Mentioned|p20|Mesoproterozoic|Mesoproterozoic|An extension of the Cu-Au-U mineralisation associated with the historic Hillside Mine has been found to occur in three fault structures within the Arthurton Granite which contain sulphide mineralisation (Zanoni, Parsee and Songvaar).||||||
29921|Arthurton Granite|69748|5|Briefly described|p179-182, 185-187, 189-198|Mesoproterozoic|Mesoproterozoic|Moonta-Wallaroo region, Olympic IOGC Province. Photomicrographs. REY fractionation trends graphed. LA-CP-MS data for REE, Pb, Th, U and other elements tabulated.|1583 +/- 7 Ma.|Hiltaba Suite.|||Forms composite batholiths comprising monzogranite and granodiorite to tonalite. A-type.|
29921|Arthurton Granite|70382|6|Mentioned|p29 Fig 3, p34|Mesoproterozoic|Mesoproterozoic|Crops out in northeastern Yorke Peninsula. Possible source for some of Quartoo Sand Member inherited zircon.|||||Granite.|
29921|Arthurton Granite|72949|6|Mentioned|p36|Calymmian|Calymmian|Olympic Domain, south. Yorke Peninsula / Eastern Eyre Peninsula. A-type (alkali-calcic) granite.|1582 +/- 7 Ma|||||
29921|Arthurton Granite|73165|6|Mentioned|p619-620, p622|Calymmian|Calymmian|Gawler Craton, Moonta Domain, northern Yorke Peninsula. Suggested to post-date local deformation.|1583 +/- 7 Ma|Hiltaba Suite||Intrudes into Wallaroo Group|Undeformed granite.|
31754|Aruhna Subgroup|22927|6|Mentioned|43|||Geol province Adelaide Geosyncline||||||
31754|Aruhna Subgroup|23211|6|Mentioned|Fig.2|||of Wilpena Group.||||||
31754|Aruhna Subgroup|24586|5|Briefly described|p50 Fig. 1, p51 Fig. 2|Adelaidean|Adelaidean|Of the Wilpena Group (Heysen Supergroup). Includes Bunyeroo Formation and Wilcolo Sandstone.  Geological Province: Adelaidean Geosyncline.||||||05-JUL-06
31754|Aruhna Subgroup|43845|5|Briefly described|Fig2 p42||Neoproterozoic|In Wilpena Group||||||12-JUL-16
31754|Aruhna Subgroup|70406|5|Briefly described|p125, p121,  Fig 5|||||Of Wilpena Group. |Includes Wilcolo Sandstone, Bunyeroo Formation, Yarloo Shale.|||
31754|Aruhna Subgroup|70407|4|Described|p101-108, p112|Neoproterozoic|Neoproterozoic|Age: Ediacaran. Reference section designated in Bunyeroo Valley between Aroona Ruins and  Wilcolo Creek. Transgressive systems tract.||Of Wilpena Group. |Includes Wilcolo Sandstone, Bunyeroo Formation.|Unconformably overlies Sandison Subgroup. Unconformably overlain by Depot Springs Subgroup.||13-MAY-16
31754|Aruhna Subgroup|73222|6|Mentioned|p6|Ediacaran|Ediacaran|Adelaide Rift Complex.||Wilpena Group, Heysen Supergroup|Bunyeroo Formation|||
31754|Aruhna Subgroup|74367|5|Briefly described|p7 Fig.6, p8, p19, p22|Ediacaran|Ediacaran|Tentatively correlated with the Mount Arrowsmith Volcanics.||Wilpena Group|Bunyeroo Formation, Yarloo Shale|||
34761|Auburn Dolomite Member|22889|4|Described|p35 & p39|Adelaidean|Adelaidean|For type section location see p39. Supersedes former Auburn Dolomite as the unit has been down graded from formation to member status, see p33 for details of change.||||||05-AUG-08
34761|Auburn Dolomite Member|64797|6|Mentioned|p153 Fig.2, p161 Tb.4|Cryogenian|Cryogenian|Adelaide Rift Complex. Lithology/rank not shown on diagram. S-isotope data.||||||
82225|Aurora Tank Suite|73230|2|Defined|p6, p9-10, p12-16|Siderian|Siderian|New name [see appendix and ASUD for definition]. Gawler Craton. Domain: Christie and Wilgena. Metamorphism at c. 2470-2390 Ma. Associated with mafic-ultramafic rocks at Aristarchus. Named after Aurora Tank on the COOBER PEDY mapsheet. Previously informally attributed to the Kenella Gneiss, Glenloth Granite or undifferentiated Mulgathing Complex. Type locality: four kilometres west of Aurora Tank. Reference drillhole: DMDD-002 (234168), interval 196-307 m. Outcrops in the northern Gawler Craton near Aurora Tank and Commonwealth Hill Outstation and occurs in drillholes in the Aristarchus prospect. Thickness: 313 m interlayered with Burden Metagabbro intersected in the reference drillhole (base not intersected), with individual granitoid layers 0.1 to 15 m thick. Magmatic age is zircon SHRIMP U-Pb from a variety of previous works. Likely temporal correlative of Kiana Granite (Dutton Suite, Sleaford Complex).|c. 2475-2470 Ma (magmatic)|Mulgathing Complex||Intrudes Christie Gneiss and Burden Metagabbro. Intruded by Aristarchus Metaperidotite.|Granitic gneiss and tabular feldspar granite with feldspar, quartz, biotite and locally hornblende.|
39515|Ayers Range Granite|60678|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Pitjantjatjara Supersuite.  Porphyritic clinopyroxene-hornblende-biotite monzonite and granodiorite.  Geological Province: Musgrave Block.||||||
39515|Ayers Range Granite|60679|5|Briefly described|Map Legend|Stenian|Stenian|Of Pitjantjatjara Supersuite. Granite monzonite, quartz monzonite. Geological Province: Musgrave Block.||||||
39515|Ayers Range Granite|61154|2|Defined|p43 App., p12-13, p29|Mesoproterozoic|Mesoproterozoic|Formerly Ayers Range adamellite. Of Pitjantjatjara Supersuite. Heterogeous granite, grey to pale grey-green, weakly to strongly porphyritic - detailed lithology in text (p12-13). Intrudes the Alcurra Dolerite.  Age: 1159+/-17Ma (U-Pb: Edgoose et  al 1993)||||||14-JUL-05
39515|Ayers Range Granite|69436|5|Briefly described|p21:9|||Edgoose et al. (2004). Formerly Ayers Range adamellite (Edgoose et al., 1993).|||||Quartz monzonite, heterogeneous, grey and porphyritic, generally with an inequigranular granoblastic texture; porphyritic microgranite; weakly foliated granite, with clinopyroxene rimmed by amphibole a ubiquitous and diagnostic feature.|12-JUL-16
41670|Babbage Supersuite|50605|5|Briefly described|p(ii), 10.1, Table 1.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Gawler Craton & Curnamona Province. Age: 1560Ma.||||||23-SEP-04
41670|Babbage Supersuite|65455|6|Mentioned|p9 Fig. 5|Mesoproterozoic|Mesoproterozoic|On the northwestern margin of the Curnamona Province. Has uranium abundances of greater than 100 parts per million (Yerila Granite on p12).||||||09-MAY-12
28340|Bakara Calcrete|23719|5|Briefly described|p30|Pleistocene|Pleistocene|Geological Province: Gawler Craton.||||||
28340|Bakara Calcrete|30757|6|Mentioned|p3|||||||||
28340|Bakara Calcrete|33834|6|Mentioned|p16|||||||||
28340|Bakara Calcrete|35097|6|Mentioned|Fig.4|||||||||
28340|Bakara Calcrete|35232|6|Mentioned|p15|||Intended informal name||||||
28340|Bakara Calcrete|39351|6|Mentioned|Map legend|Quaternary|Quaternary|||||||
28340|Bakara Calcrete|40219|6|Mentioned|p2|||||||||
28340|Bakara Calcrete|40442|5|Briefly described|p35|||||||||
28340|Bakara Calcrete|40450|6|Mentioned|p68|||||||||
28340|Bakara Calcrete|40941|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
28340|Bakara Calcrete|40942|6|Mentioned|p20|||||||||
28340|Bakara Calcrete|41619|6|Mentioned|Map legend|Pleistocene||||||||
28340|Bakara Calcrete|42498|5|Briefly described|Map Legend|Pleistocene|Pleistocene|||||||
28340|Bakara Calcrete|42499|5|Briefly described|Map legend|Pleistocene||||||||
28340|Bakara Calcrete|42506|5|Briefly described|Map legend|Pleistocene||||||||
28340|Bakara Calcrete|42716|5|Briefly described|Map legend|Pleistocene||||||||
28340|Bakara Calcrete|42720|5|Briefly described|map legend|Pleistocene||||||||
28340|Bakara Calcrete|42738|5|Briefly described|map legend|Quaternary||||||||
28340|Bakara Calcrete|42813|6|Mentioned|p25|||||||||
28340|Bakara Calcrete|42966|3|Fully described|p214|||||||||
28340|Bakara Calcrete|43049|5|Briefly described|p26|||||||||
28340|Bakara Calcrete|43094|5|Briefly described|p40|||||||||
28340|Bakara Calcrete|49038|4|Described|Table 2|||||||||
28340|Bakara Calcrete|62893|5|Briefly described|Map Legend, p24|Pleistocene|Pleistocene|Interbedded with Bridgewater Formation (Upper Member).||||Equivalent to Upper Bridgewater Formation.|Soft, less-indurated calcrete, nodules and carbonate cements.|
28340|Bakara Calcrete|65922|5|Briefly described|p25 Tb. 4, p27|Pleistocene|Pleistocene|Nodular to platy, blocky or massive calcrete developed within calcareous silty clay. Hard blocky calcrete has traditionally been called Ripon Calcrete but not differentiated in this article. Developed within most Pleistocene units in the YARDEA sheet.||||||
34786|Bald Rock beds|22755|6|Mentioned|p555|||||||||
25773|Balquhidder Formation|22643|5|Briefly described|p186, fig3,6,7|Early Cambrian|Early Cambrian|||||||
25773|Balquhidder Formation|22840|6|Mentioned|Table1 P38|||||||||
25773|Balquhidder Formation|23317|5|Briefly described|380 Fig.2|||||||||
25773|Balquhidder Formation|23539|4|Described|Fig 1 p 467|||||||||
25773|Balquhidder Formation|23996|5|Briefly described|p352 Fig.1|Cambrian|Cambrian|Of Kanmantoo Group.||||||
25773|Balquhidder Formation|24465|4|Described|p357|Early Cambrian|Early Cambrian|Of Bollaparudda Subgroup (Kanmantoo Group). Overlain by Petrel Cove Formation. See also p346 Fig. 3.||||||27-MAY-08
25773|Balquhidder Formation|30380|6|Mentioned|Table 1|||Correlation||||||
25773|Balquhidder Formation|30381|2|Defined|p217|Cambrian|Cambrian|Part of Brown Hill Sub-group||||||
25773|Balquhidder Formation|35255|6|Mentioned|Fig.8|||||||||
25773|Balquhidder Formation|36836|6|Mentioned|Table 1|||||||||
25773|Balquhidder Formation|38873|4|Described|Table 2|||||||||
25773|Balquhidder Formation|40442|6|Mentioned|Table 1|||||||||
25773|Balquhidder Formation|40454|6|Mentioned|p46|||||||||
25773|Balquhidder Formation|40455|5|Briefly described|p71|||||||||
25773|Balquhidder Formation|41947|6|Mentioned|p16|||||||||
25773|Balquhidder Formation|42222|6|Mentioned|p21|||||||||
25773|Balquhidder Formation|42225|6|Mentioned|Fig.4 P224|||||||||
25773|Balquhidder Formation|42270|6|Mentioned|p353|||||||||
25773|Balquhidder Formation|42271|6|Mentioned|Fig.5 P376|||||||||
25773|Balquhidder Formation|42788|5|Briefly described|Fig.14 P148|||of Kanmantoo Group||||||
25773|Balquhidder Formation|43703|6|Mentioned|Fig.1,p75|||||||||
25773|Balquhidder Formation|43759|6|Mentioned|p445|||||||||
25773|Balquhidder Formation|44133|5|Briefly described|p4 Fig. 7.2, 18|Middle Cambrian|Middle Cambrian|Geological Province: Stansbury Basin. Of the Kanmantoo Group. Overlain by Petrel Cove Formation.||||||
25773|Balquhidder Formation|60712|5|Briefly described|p28 Fig. 1, p36|Early Cambrian|Early Cambrian|Of the Kanmantoo Group. Interbedded phyllite and fine-grained sandstone. Conformably overlies (grades into) the Tunkalilla Formation.||||||27-MAY-08
25773|Balquhidder Formation|61046|5|Briefly described|p8 Fig. 2|Early Cambrian|Early Cambrian|Of Kanmantoo Group. Metasandstone with metasiltstone interbeds. Some units of pyritic schist.||||||
25773|Balquhidder Formation|61307|5|Briefly described|p6 Fig. 3|Cambrian|Cambrian|Geological Province: Adelaide Fold Belt.||||||
25773|Balquhidder Formation|63562|6|Mentioned|p353 Fig.11|||Detrital zircon spectrum shown in Australia/Gondwana reconstruction.||Kanmantoo Group.||||
25773|Balquhidder Formation|64282|5|Briefly described|Map legend|Early Cambrian|Early Cambrian|Of the Kanmantoo Group. Geol. province: Kanmantoo Trough. Grey, biotite-laminated, lithic metasandstone. Well-bedded to convoluted. Bouma-like sequence of alternating sandstone and siltstone, graded bedding, flame structures and ripple drift x-bedding.||||||26-JUN-08
25773|Balquhidder Formation|65375|5|Briefly described|p33.|Middle Cambrian|Middle Cambrian|||Unit in Kanmantoo Group.||Overlies Tunkalilla Formation. Is overlain by Petrel Cove Formation.||
25773|Balquhidder Formation|65664|5|Briefly described|p1096, pp1101-4 Tabs.1-4, p1106 Fig.5|Early Cambrian|Early Cambrian|Deposited in a deep water turbiditic environment.||Of Bollaparudda Subgroup.||Overlies Tunkalilla Formation. Overlain by Petrel Cove Formation.||09-MAY-12
25773|Balquhidder Formation|65892|5|Briefly described|p9 Fig.4. |Middle Cambrian|Middle Cambrian|Fleurieu Peninsula.||Unit in Kanmantoo Group.||Overlies Tunkalilla Formation. Is overlain by Petrel Cove Formation.||
25773|Balquhidder Formation|65921|6|Mentioned|p1, p2 (map legend).|Cambrian|Cambrian|Mis-spelt as Balquidder on p1.||Of the Kanmantoo Group.||||
25773|Balquhidder Formation|68735|5|Briefly described|p235 Fig.3|Middle Cambrian|Early Cambrian|Fleurieu Peninsula.||Of the Kanmantoo Group.||||10-APR-17
25773|Balquhidder Formation|68993|6|Mentioned|p544 Fig.1|Middle Cambrian|Early Cambrian|Fleurieu Peninsula.||Of the Kanmantoo Group.||||
25773|Balquhidder Formation|73107|5|Briefly described|Map legend.|Early Cambrian|Early Cambrian|Kanmantoo Trough.||Kanmantoo Group.|||Grey biotite-laminated, lithic metasandstone. Well-bedded to convoluted. Bouma-like sequence of alternating sandstone and siltstone, graded bedding, flame structures and ripple drift crossbedding.|
25773|Balquhidder Formation|74367|6|Mentioned|p16|Early Cambrian|Early Cambrian|||||||
24172|Baltucoodna Quartzite|22629|6|Mentioned|p153|Statherian|Statherian|||||||
24172|Baltucoodna Quartzite|23054|5|Briefly described|p8-9|||||||||
24172|Baltucoodna Quartzite|36733|2|Defined|p67|Paleoproterozoic|Paleoproterozoic|See also P20.||||||07-NOV-08
24172|Baltucoodna Quartzite|38108|6|Mentioned|Table 1|||||||||
24172|Baltucoodna Quartzite|43052|5|Briefly described|p101|||of Peake Metamorphics||||||
24172|Baltucoodna Quartzite|44289|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
24172|Baltucoodna Quartzite|50605|6|Mentioned|p11.3|||||||||
24172|Baltucoodna Quartzite|65376|5|Briefly described|p227.|Paleoproterozoic|Paleoproterozoic|Predominantly quartzitic sequence.||Unit in Peake Metamorphics.||||
24172|Baltucoodna Quartzite|65390|5|Briefly described|p13, p22 Fig. 3|Statherian|Statherian|Of Peake Metamorphics, Gawler Craton. Age of 1780 Ma given.||||||
24172|Baltucoodna Quartzite|66302|6|Mentioned|p30, p33|||Peake and Denison Domain, Gawler Craton. Deposited in a shallow marine setting. ||||||
24172|Baltucoodna Quartzite|71348|5|Briefly described|p200|||Mildly deformed, predominantly quartzite sequence in outcrop. Interbedded with Tidnamurkuna Volcanics.||||||
41896|Barton Sand|61234|5|Briefly described|p7 Fig. 4|Late Eocene|Late Eocene|Geological province: Eucla Basin.||||||
41896|Barton Sand|61856|6|Mentioned|p300 Fig.2, p311, p315 Fig.9, p317 |Late Eocene|Late Eocene|New name. Formerly part of the Ooldea Sand; separated due to accumulation in a separate barrier system that formed during a later sea-level rise (Tuketja transgression).||||||
41896|Barton Sand|64646|6|Mentioned|p23 Fig. 3, p24 Fig. 4|Oligocene|Eocene|Geological Province: Gawler Craton.||||||
41896|Barton Sand|67462|5|Briefly described|Map legend.|Oligocene|Eocene|Eucla Basin.||||||
41896|Barton Sand|68715|6|Mentioned|p30 Fig.5|Priabonian|Priabonian|SW and NW Gawler Craton, Eucla Basin.||||||
41896|Barton Sand|69598|6|Mentioned|p9|Early Oligocene|Late Eocene|||||||
41896|Barton Sand|70337|5|Briefly described|Map legend.|Pleistocene|Eocene||||||Sand, medium-grained, poorly cemented, beach-barrier and aeolian.|
34659|Basket Range Sandstone|22869|2|Defined|P38, P45, P46, Fig3||Neoproterozoic|New name, correlated with upper member of Skillogalee Dolomite, Formerly Aldgate Sandstone||||||
34659|Basket Range Sandstone|22889|6|Mentioned|p34|Adelaidean|Adelaidean|Parent - Mundallio Subgroup.||||||
34659|Basket Range Sandstone|61237|6|Mentioned|p36|||Used as building stone, superseding the Tapley Hill and Glen Osmond Bluestones.||||||
34659|Basket Range Sandstone|61525|6|Mentioned|p41|||Building stone.||||||
34659|Basket Range Sandstone|64769|6|Mentioned|p28|||SA. Dimension stone name.||||||06-MAY-09
35879|Basso Suite|23347|3|Fully described|p51 Tb. 1, p53 Fig. 3, p55|Paleoproterozoic|Paleoproterozoic|Characterises lower part of Willyama Supergroup, the Curnamona Group. Comprises Abminga and Ameroo Subsuites, and Ameroo Gneiss. Age: 1.69Ga and less. Albitic granofels and granite gneiss; A-type.||||||24-MAR-09
35879|Basso Suite|24307|6|Mentioned|p975 Tb. 1|||||||||
35879|Basso Suite|60485|5|Briefly described|p26|||Includes the Abminga Subsuite volcanics.||||||
35879|Basso Suite|61734|5|Briefly described|p52 Fig.2|Statherian|Statherian||1.71 Ga (U-Pb)|||Intrudes the Curnamona Group. Is intruded by Lady Louise Suite.|Albitic granofels and granite gneiss.|
35879|Basso Suite|61736|5|Briefly described|p666 Fig. 3, p673|Paleoproterozoic|Paleoproterozoic|Ages: 1713+/2, 1710+/-3, 1713+/-3Ma. Geological province: Olary Domain.||||||
35879|Basso Suite|62373|6|Mentioned|p503, p504 Fig.3|||Synsedimentary a-type.||||||
35879|Basso Suite|62514|5|Briefly described|p746, p748 Fig. 3|Paleoproterozoic|Paleoproterozoic|Intrudes the Willyama Supergroup.  A-type granitoids. Age: ca.1.71-1.70Ga. Geological Province: Olary Domain/Curnamona Province.||||||01-DEC-09
35879|Basso Suite|62535|5|Briefly described|p666, p672-673|Paleoproterozoic|Paleoproterozoic|Several age determinations given.|1713 +/- 3 Ma.|Wiperaminga Subgroup.|||Felsic metavolcanic rocks.|
35879|Basso Suite|62536|5|Briefly described|p643|||Olary Domain. Coeval with Alma Gneiss (Broken Hill area).|1720-1705 Ma.|||||
35879|Basso Suite|62592|5|Briefly described|p14, p16 Fig.2.2.|Statherian|Statherian|Olary Domain. A-type magmatism. Hosts Au-Cu deposits.|1718-1712 Ma.|||Intrudes Curnamona Group. Is cut by Lady Louise Suite.|Includes mafic volcanics.|
35879|Basso Suite|62728|5|Briefly described|p24, p28|||A set of felsic granitic gneisses and albitic granofels. A-type. The granitoid component is Ameroo Subsuite, outcropping in Olary Domain. Geol.P: Olary Domain/Curnamona Province.||||||07-FEB-11
35879|Basso Suite|62993|5|Briefly described|p2, p8, p12, p39, p40|Paleoproterozoic|Paleoproterozoic|In the form of a sill at the Mount Mulga Mine traverse.Intruded by mafic dykes (Lady Louise Sute) at Mulga Bore Creek.|1718 - 1711 Ma||Includes Ameroo Subsuite, Abminga Subsuite|Intrudes Willyama Supergroup, Curnamona Group, George Mine Formation. Intruded by Lady Louise Suite|Includes foliated A-type metagranite.|19-DEC-21
35879|Basso Suite|63020|5|Briefly described|p983, p987 Fig. 8|Paleoproterozoic|Paleoproterozoic|Consists of lavas, volcaniclastics and shallow subvolcanic granite sills of felsic A-type composition. Age: 1715-1710Ma. Geological Province: Curnamona Province.||||||07-NOV-08
35879|Basso Suite|63102|4|Described|p6,10-11,13-14,16,20,28,30-32|Statherian|Statherian|Geological province: Olary Domain, Curnamona Province. Extensive in central part of Olary Domain. A-type igneous magmatism coeval with Curnamona Group sedimentation i.e. Montstephen Basalt. Has U-Pb zircon ages including 1712+\-3 and 1713+\-3 Ma (Mulga Bore Creek), 1707+\-3 Ma (Cathedral Rock) and 1715+\-3 Ma (Mount Howden). See p39 for additional zircon U-Pb results. See also p35,38-40,52/|~1715-1710 Ma|Unit of Ethiudna Subgroup.|Includes the Abminga Subsuite and the Ameroo Subsuite.||Felsic subvolcanic intrusives, volcanics and epiclastics with possible coeval mafic volcanics.|22-OCT-19
35879|Basso Suite|63186|5|Briefly described|p71 Fig. 5|Paleoproterozoic|Paleoproterozoic|Age: 1705 Ma. Geological Province: Curnamona Province.||||||07-NOV-08
35879|Basso Suite|63224|6|Mentioned|p12|||Geological Province: Curnamona Province.||||||07-FEB-08
35879|Basso Suite|63866|4|Described|p37, p40-p41, p49|Statherian|Statherian|Olary Domain, Curnamona Province. |1710 +/- 9 Ma (Conor et al., 2006)||Includes the Amaroo Subsuite and the Abminga Subsuite.|Intrudes the Curnamona Group.||
35879|Basso Suite|64741|5|Briefly described|p301 Fig. 4, p302|Paleoproterozoic|Paleoproterozoic|Includes Abminga Subsuite. Intrudes the Curnamona Group. Age: 1719-1713Ma. Geological province: Olary Domain. A-type felsic quartz-eye volcanic units and subvolcanic granite sills intercalated with the Wiperaminga and Ethiudna Subgroups.||||||07-FEB-11
35879|Basso Suite|64742|6|Mentioned|p320, p321 Fig.3.||||c.1715-1710 Ma.|Unit in Curnamona Group.||||29-MAR-12
35879|Basso Suite|64944|5|Briefly described|p27, p28 Fig. 1|Paleoproterozoic|Paleoproterozoic|Associated with the Curnamona Group. Age: 1719-1713Ma (mainly 1718-1715Ma). Geological province: Olary Domain. A-type igneous rocks.||||||07-FEB-11
35879|Basso Suite|65220|5|Briefly described|p21 Fig.3|Statherian|Statherian|1715-1700 Ma, A-types||||||10-DEC-09
35879|Basso Suite|65375|6|Mentioned|p13.|Paleoproterozoic|Paleoproterozoic||c.1710 Ma.|||||
35879|Basso Suite|66302|5|Briefly described|p36 Fig.9, p37|Statherian|Statherian|Olary Domain, Curnamona Province. Largely A-type igneous and volcanic rocks. |ca. 1715-1719 Ma||Includes the Abminga and Ameroo Subsuites.|Intrudes the Curnamona Group.||
35879|Basso Suite|67323|5|Briefly described|Eastern Australia Time-Space Plot; p33|||Olary Domain, Curnamona Province.|1713 +/- 3 Ma to 1710 +/- 3 Ma.|||Intrudes Wiperaminga Subgroup.||
35879|Basso Suite|67536|5|Briefly described|Map Legend|Statherian|Statherian|Curnamona Province.|ca. 1712 +/- 2 Ma - 1699 +/- 10 Ma||||A-type metagranitoids and felsic metavolcanics.|02-APR-14
35879|Basso Suite|67581|6|Mentioned|p45|||||Willyama Supergroup.||||
35879|Basso Suite|67653|6|Mentioned|p4|||Geological province: Curnamona Province. |||||medium- to coarse-grained and massive, rangingM from tonalite to monzogranite, and accompanied by abundant alaskitic pegmatites.|
35879|Basso Suite|68126|6|Mentioned|p6, p26, p30|||Olary Domain, Curnamona Province.|c.1715 Ma.|||||
35879|Basso Suite|68315|6|Mentioned|p764|||Curnamona Province.|1.71 Ga.|||||
35879|Basso Suite|69562|6|Mentioned|p674 Fig.6|||||Unit in Ninnerie Supersuite.||||
35879|Basso Suite|70405|5|Briefly described|p1,p15, p33|Paleoproterozoic|Paleoproterozoic||1710 Ma - 1720 Ma|Kalabity Supersuite|Includes Abminga Subsuite, Ameroo Subsuite|Intrudes into Curnamona Group|Felsic igneous rocks.|
35879|Basso Suite|70657|4|Described|p6 Fig.1, p12, p13 Fig.6, p15-16, p18|Statherian|Statherian|See also p21, p23, p26, p30, p32, p45-47, p59. Conor (2000). Curnamona Province. Characterises Curnamona Group of Olary Domain. Regionally extensive and distinctive. In Broken Hill Domain, known only from detrital material. Various ages given between ~1718-1702 Ma. Comprises the co-magmatic (meta)granites, and (meta)rhyolitic volcanics and volcaniclastics of the Curnamona Group. Sodic alteration described.|1719-1713 Ma||Abminga, Ameroo Subsuites.|Extrusive flows in Curnamona Group (Wiperamina and Ethiudna Subgroups). Intruded by Lady Louise Suite.|Volcanics and epiclastics; granite sills. A-type.|
35879|Basso Suite|70658|5|Briefly described|p1-2, 5, 8, 11-12, 15, 29, 32, 42|Paleoproterozoic|Paleoproterozoic|Olary Domain, Curnamona Province.|1720-1710 Ma.||Abminga, Ameroo Subsuites.|Associated with the Curnamona Group.|Metagranite; felsic metavolcanics. A-type.|
35879|Basso Suite|72454|6|Mentioned|p2 Fig.2|Mesoproterozoic|Mesoproterozoic|Part of the Olary Domain. Shown only on p2 Fig.2.||||Shown as younger than Willyama Supergroup and older than Lady Louise Suite.||
35879|Basso Suite|73021|6|Mentioned|p224||||1.71 Ga.|Willyama Supergroup.||||
35879|Basso Suite|73030|6|Mentioned|p2150|Statherian|Statherian||ca. 1720-1710 Ma|||||
26375|Bayley Range Siltstone Member|22921|5|Briefly described|38|||Parent Sandison Subgroup||||||
26375|Bayley Range Siltstone Member|23287|6|Mentioned|Fig.3|||Age: Lower Ediacarian. of Sandison Subgroup.||||||
26375|Bayley Range Siltstone Member|24195|5|Briefly described|p45 Fig.3|||Of the Brachina Formation. Geological Province: Adelaide Geosyncline||||||
26375|Bayley Range Siltstone Member|30807|6|Mentioned|p102|||Suggested map symbol||||||
26375|Bayley Range Siltstone Member|34291|6|Mentioned|p20|||See also P76. Adelaidean||||||
26375|Bayley Range Siltstone Member|35586|6|Mentioned|p26|||Now to be known as Bayley Range Formation.||||||
26375|Bayley Range Siltstone Member|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Marinoan||||||
26375|Bayley Range Siltstone Member|39808|6|Mentioned|p223|||||||||
26375|Bayley Range Siltstone Member|41429|3|Fully described|p221|||||||||
26375|Bayley Range Siltstone Member|42222|6|Mentioned|p18|||||||||
26375|Bayley Range Siltstone Member|42600|4|Described|p10|||Of Brachina Formation.||||||30-SEP-08
26375|Bayley Range Siltstone Member|43052|5|Briefly described|p192,table 6.1|||of Brachina Formation||||||
26375|Bayley Range Siltstone Member|43622|6|Mentioned|p38|Neoproterozoic||||||||
26375|Bayley Range Siltstone Member|60959|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Thinly bedded siltstone and sandstone with current ripples and cross bedding.||||||
26375|Bayley Range Siltstone Member|61732|5|Briefly described|p28 Fig. 13|Marinoan|Marinoan|Of the Brachina Formation (Sandison Subgroup, Wilpena group). . Geological Province: Adelaide Rift Complex||||||07-FEB-11
26375|Bayley Range Siltstone Member|67030|6|Mentioned|p409 Fig. 2|Ediacaran|Ediacaran|||Of Brachina Formation||Overlies the Moorillah Siltstone Member, underlies the ABC Quartzite.||26-APR-12
26375|Bayley Range Siltstone Member|70406|5|Briefly described|p126, 121 Fig 5, p128.|Neoproterozoic|Neoproterozoic|||Of Brachina Formation.||Lateral equivalent of Corraberra Sandstone Member.||
26375|Bayley Range Siltstone Member|70407|5|Briefly described|p103 Fig 2|Neoproterozoic|Neoproterozoic|Age: Marinoan.||Of Brachina Formation.||||
26375|Bayley Range Siltstone Member|71129|5|Briefly described|p131|Ediacaran|Ediacaran|Of Adelaide Geosyncline.||Unit of Brachina Formation.||Correlable to Corroberra Sandstone Member/Tent Hill Fm.||
34775|Beaumont Dolomite Member|22889|5|Briefly described|p35 & p39|Adelaidean|Adelaidean|Location of type area advised p39. The Beaumont Dolomite Member superseds the former Beaumont Dolomite as the unit has been down graded from formation to member status, see p 35 for details of change.||||||
34775|Beaumont Dolomite Member|73188|5|Briefly described|p316, p325, p329|Neoproterozoic|Neoproterozoic|Mount Lofty Ranges.||Bungarider Subgroup, Burra Group||||
79612|Beda Basalt|69666|2|Defined|p24-39|Neoproterozoic|Neoproterozoic|Willouran Basic Province. Exposed around the Cultana Inlier, Stuart Shelf; widespread below Neoproterozoic cover. First mapped and described (Crawford and Hiern, 1964) as the Roopena Volcanics, which are exposed ~40km to the NW near the Roopena Homestead. Subsequent mapping showed they were not stratigraphically equivalent. Named after Beda Bore. Type locality and reference drillhole section are specified in detail. True thickness unknown; preserved thickness from 1.1m to ~550m including about 70 flows. Inferred to be supplied with magma by feeder dykes of Gairdner Dolerite. Geological and HyLogger TIR and SWIR logs. Geochemistry, age determinations detailed.||Gawler Range Volcanics.||Unconformably overlies Pandurra, Moonabie Formations and Cultana Subsuite. Interbedded with Backy Point Formation. Is overlain unconformably by Tapley Hill Formation.|Continental flood tholeiite succession of subaerial, amygdaloidal to massive basalt flows, interbedded with fluvial sandstones and conglomerates. Substantially altered; primary igneous textures well-preserved. Sporadic brecciated flow tops.|
79612|Beda Basalt|70334|4|Described|p2,8,17,20,38-39,41-44,47,76,81-82,86-87|Tonian|Tonian|Geological province: Gawler Craton. Of Cariewerloo Basin, Stuart Shelf. Part of the Willouran Basic Province (Crawford and Hilyard, 1990). Emplaced during a major NE-SW extensional event, which was followed by continental rifting and the break-up of the supercontinent Rodinia (Crawford and Hilyard, 1990, Zhao et al., 1994, Li et al., 1999, Wang et al., 2010). Best exposed along the coast of Cultana Inlier at Backy Point, Two Hummock Point and north of Douglas Point. Extends in the subsurface N-S from Cultana Fault west to North Whyalla Hills, northwards onto AUGUSTA AND TORRENS. Deposition during early Willouran (early Neoproterozoic), after uplift of the Cultana Inlier. Substantially altered by secondary minerals chlorite, haematite and potassium feldspar. Thickness of infividual basalt flows range from 1-30m. Contemporaneous with Gairdner Dolerite. Displays close affiliation to a mixed lithospheric-asthenospheric mantle source, which may have assimilated crustal material en route. Age is inferred to be 827+\-6 Ma based on correlation with Gairdner Dolerite, but previous geochronological analysis have yielded wide-ranging and inconsistent results e.g. 697+\-34 Ma (whole Rock Rb-Sr; Webb and horr 1978), 1076+\-34 Ma (whole rock Rb-Sr; Webb and Coats 1980).||||Overlain unconformably by Tapley Hill Formation. Underlain unconformably by Moonabie Formation or Cultana Subsuite or Pandurra Formation. Interlayered with Backy Point Formation.|Subaerial tholeiitic amygdaloidal basalt, minor components of heavy mineral-banded quartzite, chert, banded iron formation, crystalline haematite and gneiss, and minor iron oxides.|14-OCT-19
79612|Beda Basalt|70948|6|Mentioned|p973|Neoproterozoic|Neoproterozoic|Geological province: Gawler Craton.||||||
79612|Beda Basalt|71037|5|Briefly described|p22-23 Fig.2, p27 Fig.6|Neoproterozoic|Neoproterozoic|Shown as isolated outcrop in the south east of the Six Mile Hill 1:75,000 surface geology map (p22-23 Fig.2). Shown as Willouran age [?Tonian].||||Partially equivalent to Backy Point Formation, Gairdner Dolerite.|Basaltic lava, locally amygdaloidal, with pyroxene.|
79612|Beda Basalt|71129|3|Fully described|p1,15,95,98-103,105-109,184|Tonian|Tonian|Of Stuart Shelf. Part of the Willouran Basic Province, which also includes the Wooltana, Cadlareena and Noranda volcanics, Wilangee Basalt and Little Broken Hill Gabbro, and Gairdner Dolerite. Related to the Rodinian break-up (Zhao et al., 1994, Li et al., 1999, Wang et al., 2010). Basaltic volcanism interpreted to be result of mantle plume upwelling, causing doming in the continental lithosphere (Zhao et al., 1994). Reference drillhole: PSH 1/ SAS 1 (drillhole 136943); intersecting 22 individual lava flows, ranging in thickness from less than 1 to 30m (Wade and McAvaney, 2014). Combined thickness with Backy Point Formation indicates thickening from west to east. Drilled sections in SIXMILE HILL range in thickness from <30m in the SE, up to 197m of Beda Basalt in the NE (PSH 1 / SAS 1 drillhole). Original thickness is unknown as it was exposed to erosion on the Stuart Shelf during Burra Group deposition in the Adelaide Geosyncline (Preiss 2000). Interlayered nature with fluvial Backy Point Formation indicate a subaerial emplacement, supported by presence of peperitic contacts with Backy Point Formation, showing contact with wet unconsolidated sediment. Age is not well-constrained due to unsuitability of U-Pb dating, and being bounded by unconformities. Previous attempts at Rb-Sr and Ar-Ar geochronology yielded inconsistent results. Preferred age is 827+\-6 Ma, based on correlation and Gairdner Dolerite. See also p207-208,225,227.|c. 827 Ma|Unit of Callanna Group.||Unconformably overlain by Tapley Hill Formation or Moonlight Conglomerate. Intercalated with Backy Point Formation. Contemporaneous with Gairdner Dolerite. Underlain by Pandurra Formation.|Subaerial tholeiitic lavas; massive to amygdaloidal. Flow tops and bottoms most commonly marked by red-brown fine-grained basalt containing amygdales filled with chlorite, calcite, quartz, potassium feldspar, albite and/or specular hematite.|13-NOV-19
79612|Beda Basalt|71130|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Age given as Willouran.||||Interbedded with Backy Point Formation.|Basalt.|
79612|Beda Basalt|71131|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Age given as Willouran.||||Interbedded with Backy Point Formation.|Basaltic lava, locally amygdaloidal, with pyroxene.|
79612|Beda Basalt|71712|6|Mentioned|p411, p413 Fig 2, p415, p418|Tonian|Tonian|Also refererd to as Beda Volcanics in p413 Fig 2, p415. Age from Gairdner Dolerite.||||Underlain by Pandurra Formation. Coeval with Gairdner Dolerite. Interfingered with Backy Point Formation.||31-MAR-20
79612|Beda Basalt|71895|4|Described|p10, p11 fig 2, p23, p29, p54|Neoproterozoic|Neoproterozoic|This is the volcanic equivalent of the Gairdner Dolerite. Flow top breccias are common. Spectral analysis is provided. See the also the Beda Volcanics. See also p61, p116, p122, p141-p144, p150-p151, APP1. p87-p97, APP4. p4,  APP4. p8.||||Overlies the Pandurra Formation. Unconformably overlain by the Umberatana and Wilpena groups.|Fine- to medium-grained, amygdaloidal, purple to grey-black basalt that is often strongly altered.|
79612|Beda Basalt|72090|5|Briefly described|p34, p36-p37, p107-p108|||Gawler Craton. Calcite veins are common.||||Overlain by the Tapley Hill Formation.|Greenish grey to pale reddish brown, amygdaloidal fine- to medium-grained basalt.|
79612|Beda Basalt|72242|6|Mentioned|p27|Tonian|Tonian|Geological province: Coompana Province, Western Gawler Craton.||||||
79612|Beda Basalt|72247|5|Briefly described|p43|Neoproterozoic|Neoproterozoic|Of Adelaide Geosyncline.||||Transitional to Beda Basalt. Overlain by Brighton Limestone.||
79612|Beda Basalt|73110|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic||||||Basaltic lava, locally amygdaloidal, with pyroxene.|
79612|Beda Basalt|73188|6|Mentioned|p315|||Accompanied earliest rifting in the Adelaide Geosyncline.||||||
79612|Beda Basalt|73226|6|Mentioned|p3-4|||||||Overlain by Tapley Hill Formation.||
79612|Beda Basalt|73227|5|Briefly described|p24-25, p35|Tonian|Tonian|Stuart Shelf, south-eastern. Sturtian. Tholeiitic. Has yielded a wide range of conflicting ages but c. 830 Ma is generally accepted. Dykes of the Gairdner Dolerite are interpreted as feeders for this unit. Possible metal-rich source rock.|c. 830 Ma|Umberatana Group||Underlain by Pandurra Formation. Overlain by Tapley Hill Formation. Equivalent to Backy Point Formation and Gairdner Dolerite.||
79612|Beda Basalt|73234|6|Mentioned|p6|||Contemporaneous with Gairdner Dolerite.||||||
79612|Beda Basalt|74367|5|Briefly described|p18-19|||Willouran Basic Province. Previously the Beda Volcanics. Neither Rb-Sr isochron age has been substantiated. Suggested to be coeval with Gairdner Dolerite (827+/-6 Ma, Wingate et al., 1998).|697+/-70 Ma and 1076+/-34 Ma Rb-Sr whole rock|||Underlies Tapley Hill Formation, 'Willochra Subgroup'. Correlated with Wooltana Volcanics||
75867|Benagerie Volcanic Suite|67540|3|Fully described|p25-28: Fig.1; p36-39: Tb.3, Fig.2|Calymmian|Calymmian|Named after Benagerie Ridge. Type locality: Drillholes Mudguard 1 and BRD003. Curnamona Province: Mudguard Domain and Moorowie Sub-basin -  Erudina Domain. ~1.5km thick (in seismic). Definition reference: Fricke and Hore (2011). Originally reserved as 'Benagerie Volcanics' by Conor (Nov.2005). Dated using SHRIMP I and II (Fanning et al. 1998; Jagodzinski and Fricke 2010; Fricke et al. in prep).|1587-1581 Ma |Of the Ninnerie Supersuite.|Includes Finlay Dam Rhyolite, Lake Elder Rhyodacite, and unnamed subunits of the Benagerie Volcanic Suite: Benagerie 1 (a dacite) and Benagerie 2 (a volcanic breccia body).|Unconformably overlies Willyama Supergroup.|Volcanic or subvolcanic rocks of generally A-type composition: porphyritic rhyolite to rhyodacite and porphyritic amygdaloidal dacite, and basaltic to andesitic breccia.|08-FEB-16
75867|Benagerie Volcanic Suite|67900|4|Described|p17-19, 21-22, 24-32|Mesoproterozoic|Mesoproterozoic|Benagerie Ridge region, Mudguard Domain, Curnamona Province. Appears in text as BVS after first mention. The upper part shares geochronological, geochemical and isotopic affinities with Gawler Range Volcanics (elaborated in this study), implying joint membership of a formerly contiguous silicic large igneous province. 1587 - 1584 Ma. Totally under cover. Flat-lying and relatively undeformed. Geochemistry extensively detailed.|1581 +/- 4 Ma (SHRIMP U-Pb; Fanning et al., 1998).|Ninnerie Supersuite.|Finlay Dam Rhyolite, Lake Elder Rhyodacite.|Overlies Willyama Supergroup.|A flat-lying sheet of A-type felsic volcanic rocks. Generally porphyritic; composition ranges from rhyolite to dacite. An unnamed subunit comprises amygdaloidal basalt interlayered with sandstone and siltstone; also peperitic basalt.|
75867|Benagerie Volcanic Suite|69562|5|Briefly described|p672 Tb.5|||Appears as Benagerie Volcanics in Fig.6.|c.1587 Ma.||Includes Finlay Dam Ryolite, Lake Elder Rhyodacite.|||
75867|Benagerie Volcanic Suite|69650|2|Defined|p4 Tb.1; p2; p7-8,10 Tb.2; p11, p13, p38|Calymmian|Calymmian|See also p41, p44-57. Named after Benagerie Ridge. Mudguard Domain and Erudina Domain. Originally reserved as Benagerie Volcanics (Conor, 2005). Type sections in drillholes Mudguard 1 and BRD 003 (see both Members). Thickness of ~1.5km interpreted from seismic data. Also includes an unnamed dacite subunit and an unnamed breccia unit. Older age by Jagodzinski and Fricke (2010); younger from Fanning et al. (1998). Intruded by [?]comagmatic granites of the same age: 1590 +/- 6 Ma (Fraser and Neumann, 2010). Geochemistry detailed.|1587 +/- 6 Ma and 1581 +/- 4 Ma.|Unit in Ninnerie Supersuite.|Includes Lake Elder Rhyodacite and Finlay Dam Rhyolite.|Unconformably overlies folded Willyama Supergroup.|Porphyritic rhyolite to rhyodacite and porphyritic, amygdaloidal dacite, and basaltic to andesitic breccia. A-type.|25-NOV-22
75867|Benagerie Volcanic Suite|70383|6|Mentioned|p47|||Central Curnamona Province. Unmetamorphosed. Mentioned as a possible source of porphyritic rhyolite clasts in the Sprigg Diamictite Member.||||||
75867|Benagerie Volcanic Suite|70658|5|Briefly described|p33, 35|Mesoproterozoic|Mesoproterozoic|Benagerie Ridge, Mudguard Domain, Curnamona Province. Geochemistry briefly described.|1587-1581 Ma.|Ninnerie Supersuite.|Lake Elder Rhyodacite, Finlay Dam Rhyolite.|Overlies Coulthard Suite.|A-type, sub-surface felsic volcanics. Porphyritic rhyolite to rhyodacite and porphyritic amygdaloidal dacite, and basaltic to andesitic breccia.|
75867|Benagerie Volcanic Suite|70659|5|Briefly described|p2-3, p47-48|||Associated with plutonic rocks of the Ninnerie Supersuite. Curnamona Province. Basalts from drillhole Bumbarlow 1 are isotopically similar to Roopena Basalt.|c.1585 Ma.|||Equivalent to Gawler Range Volcanics.||06-FEB-17
75867|Benagerie Volcanic Suite|70816|6|Mentioned|p4|Calymmian|Calymmian|Geological province: Curnamona Province.|~1585 Ma|||Equivalent to the Gawler Range Volcanics. Associated with plutons of the Ninnerie Supersuite.||
75867|Benagerie Volcanic Suite|70947|6|Mentioned|p960|Calymmian|Calymmian|Geological province: Curnamona Province.|ca. 1590 Ma|||||
75867|Benagerie Volcanic Suite|71043|6|Mentioned|p104|Calymmian|Calymmian|Gawler Craton.|c.1590 Ma.|||||
75867|Benagerie Volcanic Suite|71317|6|Mentioned|p20|||Curnamona Province.||||||
75867|Benagerie Volcanic Suite|72462|6|Mentioned|p1-2, p5|Calymmian|Calymmian|Curnamona Province. Part of a silicic large igneous province; originally contiguous with the Gawler Range Volcanics and Hiltaba Suite.|ca 1586 Ma|||||
75867|Benagerie Volcanic Suite|72949|6|Mentioned|p34-35, p39|Calymmian|Calymmian|Part of the Gawler Siliceous Large Igneous Province. Shown as BV, in Curnamona Province in Fig. 3a p35, although map key gives BVS as Benagerie Volcanics Suite.|ca. 1.59 Ga|||Felsic lavas are temporally equivalent to the upper Gawler Range Volcanics.||
75867|Benagerie Volcanic Suite|73030|6|Mentioned|p2148-2150, p2153|Calymmian|Calymmian|Curnamona Province. Extensive bimodal A-type volcanic rocks. Associated with the Ninnerie Supersuite.|ca. 1590 Ma||||Bimodal volcanic rocks.|
75867|Benagerie Volcanic Suite|73155|6|Mentioned|p264 Fig.1|Calymmian|Calymmian|Curnamona Province.|ca. 1590 Ma|||||
75867|Benagerie Volcanic Suite|73162|6|Mentioned|p448, p449|Mesoproterozoic|Mesoproterozoic|Curnamona Province. Part of Gawler Silicic Large Igneous Province.|1587 Ma|||||
75867|Benagerie Volcanic Suite|73235|6|Mentioned|p52|Calymmian|Calymmian||c. 1590 Ma|||||
75867|Benagerie Volcanic Suite|73249|5|Briefly described|p316, p317 Fig.1, p335, p338|Mesoproterozoic|Mesoproterozoic|Abbreviated to BVS in text. Potential sediment source for the Lower Cretaceous Eromanga Basin.|||||Felsic volcanic rocks, predominantly rhyolite and dacite, minor basalts.|
75867|Benagerie Volcanic Suite|73516|5|Briefly described|p2, p3 Fig.1, p4, p7 Fig.7|Calymmian|Calymmian|Curnamona Province. Large igneous province. Approximately aligned with/centred over the Curnamona Conductor in magnetotelluric data. See also Benagerie Volcanics, Benagerie Suite Volcanics p1, Benagerie Ridge Volcanic Suite p8.|1595-1575 Ma|||Unconformably overlies Upper Willyama Supergroup||
75867|Benagerie Volcanic Suite|74361|6|Mentioned|p163|Mesoproterozoic|Mesoproterozoic|Curnamona Province. Contemporaneous with Gawler Range Volcanics.||||||
34750|Benbournie Dolomite Member|22889|5|Briefly described|p39|Adelaidean|Adelaidean|See p39 for location of type section and details of new stratigraphic unit. The Benbournie Dolomite Member superseds the former Benbournie Dolomite as the unit has been down graded from formation to member status, see p33 for details of change.||||||
23375|Benda Siltstone|22510|5|Briefly described|p38, Table1p37|||Of the Yudnamutana Subgroup.  Age: Sturtian||||||13-OCT-04
23375|Benda Siltstone|22631|6|Mentioned|p177|Cryogenian|Cryogenian|||||||
23375|Benda Siltstone|23351|5|Briefly described|283|Neoproterozoic|Neoproterozoic|||||||
23375|Benda Siltstone|23477|5|Briefly described|p49 Fig 3|Neoproterozoic|Neoproterozoic|Geological Province: Curnamona Province.||||||
23375|Benda Siltstone|30178|6|Mentioned|p19|||||||||
23375|Benda Siltstone|30799|2|Defined|p1|Adelaidean|Adelaidean|Correlates with Braemar Iron Fm. See also P2.||||||
23375|Benda Siltstone|30801|6|Mentioned|p5|||Sturtian. See also P6. On table only||||||
23375|Benda Siltstone|30807|6|Mentioned|p103|||Suggested map symbol||||||
23375|Benda Siltstone|30810|6|Mentioned|p2|||||||||
23375|Benda Siltstone|32635|5|Briefly described|p3|||||||||
23375|Benda Siltstone|33474|6|Mentioned|Fig.2|||||||||
23375|Benda Siltstone|35200|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
23375|Benda Siltstone|35232|6|Mentioned|p5|||See also Table 1.||||||
23375|Benda Siltstone|37461|5|Briefly described|p339|||See also Table 5.I||||||
23375|Benda Siltstone|37932|6|Mentioned|p539|||||||||
23375|Benda Siltstone|38157|6|Mentioned|Table IV|||||||||
23375|Benda Siltstone|39344|6|Mentioned|Map legend|Precambrian|Precambrian|Sturtian||||||
23375|Benda Siltstone|39352|6|Mentioned|Map legend|Precambrian|Precambrian|Sturtian||||||
23375|Benda Siltstone|40294|6|Mentioned|p41|||||||||
23375|Benda Siltstone|41405|4|Described|p136|||Mention Table 12||||||
23375|Benda Siltstone|42090|5|Briefly described|p25|||||||||
23375|Benda Siltstone|42098|5|Briefly described|p53|||||||||
23375|Benda Siltstone|42222|5|Briefly described|p15|||||||||
23375|Benda Siltstone|42272|6|Mentioned|p402|||||||||
23375|Benda Siltstone|42720|5|Briefly described|map legend|Sturtian||||||||
23375|Benda Siltstone|42813|4|Described|p18|||Of Umberatana Group.||||||30-SEP-08
23375|Benda Siltstone|43052|5|Briefly described|p183,Table 6.1|||||||||
23375|Benda Siltstone|43595|5|Briefly described|p546|||||||||
23375|Benda Siltstone|44133|5|Briefly described|p54|Adelaidian|Adeladian|||||||
23375|Benda Siltstone|61732|5|Briefly described|p28 Fig. 13|Sturtian|Sturtian|Of the Yudnamutana Subgroup (Umberatana Group). Geological Province: Adelaide Rift Complex.||||||07-FEB-11
23375|Benda Siltstone|62592|5|Briefly described|p50 Table 5.1, p58.|Sturtian|Sturtian|Adelaide Geosyncline. Combined thickness (with Pualco Tillite) of about 3 km.||Unit in Yudnamutana Subgroup.||Overlies Pualco Tillite. Is unconformably overlain by Wilyerpa Formation.|Siltstone, ironstone, dropstones.|
23375|Benda Siltstone|62724|5|Briefly described|p17 Fig. 4|Sturtian|Sturtian|Contains the Old Boolcoomata Conglomerate Mbr. Siltstone, ironstone. Unconformably overlain by Wilyerpa Fm. Geol Prov: In the MacDonald Corridor between the Bimbowrie and Kalabity Inliers/Curnamona Province. See also p16 Fig. 2.||||||07-FEB-11
23375|Benda Siltstone|62993|6|Mentioned|p5, p3, p44|Neoproterozoic|Neoproterozoic|Sturtian age.|||Includes Old Boolcoomata Conglomerate Member||Includes diamictite.|19-DEC-21
23375|Benda Siltstone|63102|5|Briefly described|p8,46|Neoproterozoic|Neoproterozoic|Geological province: Curnamona Province.||Unit of Yudnamutana Group.||Overlain unconformably b Wilyerpa Formation.|Siltstone, ironstone.|
23375|Benda Siltstone|70031|5|Briefly described|p245|Cryogenian|Cryogenian|Adelaide Geosyncline. Associated with Sturtian glaciation.||Unit of Yudnamutana Subgroup.||Overlain by Wilyerpa Formation and Warcowie Dolomite Member. Underlain by Pualco Tillite.||
23375|Benda Siltstone|70405|5|Briefly described|p2, p14 figure 6, p51 table 4|Neoproterozoic|Neoproterozoic|Shallow water sedimentary structures are preserved and include wave and current ripples, small cross beds and small scours. Dropstones present throughout. See also p52, p80, p81,  p97.||Yudnamutana Subgroup||Overlies Pualco Tillite.|Commonly laminated siltstone interbedded with clean, feldspathic, cross bedded sandstone, granite dominated conglomerate, sedimentary ironstone, arkosic grit, sedimentary breccia, diamictite and minor dolomite and limestone that is commonly pebbly.|
23375|Benda Siltstone|70657|5|Briefly described|p9 Fig.3, p54|Neoproterozoic|Neoproterozoic|||Yudnamutana Subgroup||Is overlain unconformably by Wilyerpa Formation.|Siltstone, ironstone.|
23375|Benda Siltstone|70658|6|Mentioned|p14|Neoproterozoic|Neoproterozoic|||Yudnamutana Subgroup.|||Siltstone, ironstone.|
23375|Benda Siltstone|73093|5|Briefly described|map legend|Neoproterozoic|Neoproterozoic||||||Siltstone, dark and medium grey, calcareous, laminated; minor silty limestone.|09-DEC-21
81797|Bendieuta Member|72429|3|Fully described|p952, p956, p960-963, p965, p969, p976|Lower Cambrian|Lower Cambrian|Mount Chambers Gorge, eastern Flinders Ranges. Up to 116m thick in measured section. Previously used as the Bendieuta Formation, this work confirms its member level status. Accessible exposures of the Bendieuta Member are in the southeastern ravines of the map area. The member is massive with beds 2-5m thick of peloidal and fenestral limestones, calcarenites (grains to 0.5mm) and oolites, with broad large-scale cross-bedding rich in siliciclastic silt, sand and quartz granules. Well-formed ripple marks and distinctive pale-yellow dolomitic siltstone clasts are common features of the sediments. Silt influx occurred in repeated cycles, giving a mottled appearance to the beds, and is associated with the abundant coarse-to-very coarse, well-rounded quartz sand and granules, as well as distinctive red feldspar granules up to 3mm in diameter. Most of the clastic material may be eolian and transported to the shelf as migrating dunes, or by sandstorms. Fossils are sparse in the unit and apart from small brachiopods near the base, are limited to rare transported archaeocyath fragments. Stylolites, generally sub-parallel to bedding, are common. Similar dolostone cobbles have been found elsewhere in the clastic limestone sands of Unit 3 and are evidence for dessication and rip-up on intertidal flats. The contact with unit 4, above, is somewhat sharp with little indication of a gradual transition. May be disconformably or unconformably overlain. Records the transition to a high-energy shallow marine facies at the base of the member marking the decline of regional marine transgression and the first pulse of a regressive offlap, or lowering of the sea level, that continued through to the marine and continental red beds of the Billy Creek Formation.  Limestones are potentially excellent reservoirs for hydrocarbons. Petrography, formation, weathering and internal variations are discussed at length.||Mernmerna Formation|||Massive, thick-bedded, peloidal to part oolitic and fenestral limestones with abundant silty, cross-bedded, rippled, quartz granule-interbeds. Silty dolostone intraclasts. Sparse fauna, including brachiopods, and rare transported arhcaeocyaths.|
24179|Benitos Clay|23054|6|Mentioned|p31|||||||||
24179|Benitos Clay|38604|6|Mentioned|Map legend|Quaternary|Quaternary|||||||
24179|Benitos Clay|38605|4|Described|p40|||||||||
24179|Benitos Clay|40926|6|Mentioned|p30|||||||||
24179|Benitos Clay|44133|5|Briefly described|p243|Quaternary|Quaternary|Thickness: ~1m. ||||||
24179|Benitos Clay|61155|5|Briefly described|p17|Pleistocene|Pleistocene|Overlies the Wintrena Formation. Thickness: 2m. Geological region: Oodnadatta area. ||||||
69206|Beverley Clay|60564|5|Briefly described|p4|||Overlain by Willawortina Formation.||||||
69206|Beverley Clay|65194|5|Briefly described|p47|||Overlies Beverley Sands (informal?) where present. Widespread; consists of hard, grey and brown clay with minor silt and sandy-clay interbeds||Uppermost  subunit of Namba Formation.||||08-APR-16
69206|Beverley Clay|65925|5|Briefly described|p17, p57, p59, p65.|Miocene|Miocene|||Unit in Namba Formation.|||Clay with minor alunite.|
69206|Beverley Clay|68157|6|Mentioned|p22|Miocene|Miocene|Upper seal to the Beverley sand unit, a confined aquifer which is the principal host to U mineralisation at the Beverley deposit.||Unit in Namba Formation.||||
69206|Beverley Clay|69562|6|Mentioned|p662 Tb.2, p675|||Electrical conductivity value used in forward modelling: 630 mS/m.||Unit in Namba Formation.||Overlies Beverley Sands.||08-APR-16
79323|Bewooloo Member|70405|4|Described|p21|Paleoproterozoic|Paleoproterozoic|||Toraminga Formation||Intruded by Montstephen Subsuite|Metabasalt and basalt conglomerates with exhalative metasediments.|
79323|Bewooloo Member|70658|5|Briefly described|p28|Paleoproterozoic|Paleoproterozoic|Olary Domain, Curnamona Province. Isoclinally folded.|~1718 Ma.|Toraminga Formation.|||A fragmental unit containing poorly sorted debris. Highly variable lithologies including unique altered mafic pillows set in a magnesian carbonate matrix; also Mn-rich chemical sediments (exhalites).|
30517|Big Lake Suite|13497|5|Briefly described|p75, p84|Carboniferous|Carboniferous|Commonly mistaken as Merrimelia Formation rocks. |||||Granites.|
30517|Big Lake Suite|22527|4|Described|p 2, 3, 4, 5||Carboniferous|Replaces Tirrawarra Sandstone in Moomba Field.  Geological province: Cooper Basin.||||||02-JUL-14
30517|Big Lake Suite|23154|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Geological Province - Cooper Basin.  U-Pb SHRIMP ages of 323+/-5 Ma and 298+/-4 Ma.||||||
30517|Big Lake Suite|23155|5|Briefly described|p12|Early Carboniferous|Early Carboniferous|Radiometric ages 310+/-17, 342+/-28 Ma were obtained from two samples by U-Pb dating of zircons.||||||
30517|Big Lake Suite|23344|5|Briefly described|40|Late Carboniferous|Late Carboniferous|||||||
30517|Big Lake Suite|43201|2|Defined|p8|Early Carboniferous|Late Devonian|SHRIMP ages: 298+/-4, 323+/-5 Ma. Warburton Basin.||||||
30517|Big Lake Suite|44133|6|Mentioned|p60|||||||||
30517|Big Lake Suite|60664|5|Briefly described|p40|Carboniferous|Carboniferous|Age is mid-Carboniferous.  Deeply buried under the Cooper, Eromanga and Lake Eyre Basins.||||||
30517|Big Lake Suite|60717|5|Briefly described|p39, p40-41|Carboniferous|Carboniferous|Basement rocks to Cooper Basin. Granite intrusives.  Age is Middle Carboniferous.||||||
30517|Big Lake Suite|62537|5|Briefly described|p190, p191 Fig.2, p193, p197, p200. |Carboniferous|Carboniferous|Intruded the Warburton Basin before the deposition of the Cooper and Eromanga Basins. Overlain by Late Carboniferous clastic sediments; the intrusion-uplift-burial cycle was completed within a very short interval (ca. 5 - 10 My). Highly radiogenic; produces surface heat flow over 120mW/m2.|323 +/- 5 to 298 +/- 4 Ma (Gatehouse et al. 1995).||||Granites.|
30517|Big Lake Suite|63056|5|Briefly described|p80, p81 Fig. 2|Carboniferous|Early Carboniferous|Intrusive granodiorites. Geological Province: Warburton Basin. Age is Middle Carboniferous - 330-310Ma.||||||06-FEB-07
30517|Big Lake Suite|65382|5|Briefly described|p717 App. 2|Serpukhovian|Serpukhovian|Granites, Warburton Basin. Age of 323 +/- 5 Ma. Overlain by Cooper Basin sediments from ~300 Ma. See also Big Lake granites.||||||07-MAR-12
30517|Big Lake Suite|65489|5|Briefly described|p19, p26, p28, p84, p96, p117, p120|Carboniferous|Carboniferous|Eastern Warburton Basin. Alice Springs Orogeny. SHRIMP ages from Moomba 1 and MacLeod 1, respectively. Granodiorite underlying the Nappamerri Trough produces a prominent gravity low. Appears as Big Lake suite on p28.|323 +/- 5 Ma, 298 +/- 4 Ma: Gatehouse et al. 1995||||S-type granites.|
30517|Big Lake Suite|68731|5|Briefly described|p170 Fig 3.83, p171|Cisuralian|Mississippian|Contains granite intrusives (310-330 Ma). Geochronology by Gatehouse, Fanning and Flint (1995).|323 +/- 5 Ma and 298 +/- 4 Ma (SHRIMP).|||||02-JUL-14
30517|Big Lake Suite|69019|5|Briefly described|p145-146.|||Intrudes Warburton Basin sedimentary rocks. Rb-Sr zircon ages: Gravestock et al. (1995).|310 +/- 17 Ma and 342 +/- 28 Ma.|||Intrudes Kalladeina and Pando Formations.|Granite plutons.|
30517|Big Lake Suite|69023|5|Briefly described|p149, p165|Carboniferous|Carboniferous|Gatehouse et al. (1995). A number of granite plutons underlying the Cooper Basin and intruding Warburton Basin sedimentary rocks. U-Pb zircon ages by Gatehouse et al. (1995). Currently undergoing geothermal energy testing: ~250 degrees C at a depth of c.4300 m.|342 +/- 28 Ma and 310 +/- 17 Ma.|||Intrudes Kalladeina and Pando Formations.||
30517|Big Lake Suite|69728|6|Mentioned|p284-285, 290, 295, 298-300|||Nappamerri Trough. Abbreviated to BLS for most of the article. Highly radiogenic: up to 144 ppm Th and 30 ppm U. These ages are from the western (Moomba 1) and eastern (McLeod 1) cupolas respectively. Photomicrographs.|298 +/- 4 Ma and 323 +/- 5 Ma.||||A-type granites, pervasively altered (illite comprises ~50% of the rock mass).|
30517|Big Lake Suite|69797|5|Briefly described|p17 Fig.2|Carboniferous|Carboniferous|Age: Middle Carboniferous. Geol. Prov: Warburton Basin.|||||Granite intrusives.|
30517|Big Lake Suite|69948|6|Mentioned|p3|Carboniferous|Carboniferous|Moomba area. These SHRIMP age determinations (Gatehouse et al., 1995) correspond to Alice Springs and Kanimblan Orogenies.|323 +/- 5 Ma; 298 +/- 4 Ma.||||Granites.|
30517|Big Lake Suite|69982|4|Described|p42-43, p10, p13, p17-19, p51-52, p54-55|||See also p57, p141, p154, p223-224, Appendix 1. Gatehouse et al. (1995). Moomba Field, Warburton Basin. Altered granodiorite of this unit was misidentified as Tirrawarra Sandstone (of the overlying Cooper Basin), leading to drilling into Warburton Basin rocks. Several age determinations are given from a variety of wells. Reservoir potential and attributes described. Brief thin section descriptions. Composite logs shown. Details of wells with hydrocarbon shows.|305-362 Ma (U-Pb zircon).|||Intrudes Lycosa Formation.|Granodiorite with related microdiorite or microtonalite.|12-NOV-15
30517|Big Lake Suite|70383|5|Briefly described|p51|Permian|Carboniferous|Within [intrudes?] eastern Warburton Basin.|323 +/- 5 Ma to 298 +/- 4 Ma.|||||15-JAN-19
30517|Big Lake Suite|70673|5|Briefly described|p57|||Underlies the Cooper Basin.|c.323 Ma to c.298 Ma.||||Granites.|
30517|Big Lake Suite|70823|5|Briefly described|p13-p14, p34, p36-p38, p52|||A number of zircon ages from Middleton et al. 2014a gave ages from 421 +/- 4 Ma, 345 +/- 15 Ma to 274 +/- 12 Ma. These differing ages and the age relationships of granites of this suite with overlying sedimentary rocks are yet to be resolved.||||||
30517|Big Lake Suite|73251|6|Mentioned|p62|Carboniferous|Carboniferous|Intruded the Warburton Basin.||||||
79825|Bight Basin Group|69632|5|Briefly described|p26|Cretaceous|Cretaceous||||Madura, Loongana Formations.|Is overlain by the Eucla Group.||
28168|Bijerkerno Metasediments|22553|5|Briefly described|fig2p77|Proterozoic|Proterozoic|Part of Willyama Supergroup.||||||11-JUN-08
28168|Bijerkerno Metasediments|22575|6|Mentioned|p179 Fig.2|||Of the Paragon Group, Broken Hill Block.||||||11-JUN-08
28168|Bijerkerno Metasediments|22771|5|Briefly described|Table12.2p45,47|||||||||
28168|Bijerkerno Metasediments|22857|4|Described|p45 Tb. 12.2, p388 App1 Tb. A1.1|Paleoproterozoic|Paleoproterozoic|Supersedes the Bijerkerno Beds. Of the Paragon Group. Max. thickness: 700m. Geological Province: Willyama Fold Belt.||||||07-NOV-08
28168|Bijerkerno Metasediments|22884|6|Mentioned|p47|||Geological province: Broken Hill Domain.||||||26-MAR-09
28168|Bijerkerno Metasediments|22963|5|Briefly described|p69||Paleoproterozoic|Possible correlation with Mt Isa Soldiers Cap Group and Georgetown (Qld) Etheridge Group upper sequence.||||||07-NOV-08
28168|Bijerkerno Metasediments|22965|6|Mentioned|p14,Fig1||Statherian|||||||
28168|Bijerkerno Metasediments|22967|6|Mentioned|p39||Statherian|||||||
28168|Bijerkerno Metasediments|23248|5|Briefly described|Fig2p169|||||||||
28168|Bijerkerno Metasediments|24307|5|Briefly described|p974|Paleoproterozoic|Paleoproterozoic|Of the Paragon Group.||||||07-NOV-08
28168|Bijerkerno Metasediments|38969|4|Described|p211|||||||||
28168|Bijerkerno Metasediments|39662|2|Defined|p437|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
28168|Bijerkerno Metasediments|40822|6|Mentioned|Fig.2|||||||||
28168|Bijerkerno Metasediments|41093|6|Mentioned|p252|||||||||
28168|Bijerkerno Metasediments|41630|6|Mentioned|Fig.1.3|||||||||
28168|Bijerkerno Metasediments|42261|6|Mentioned|Fig 1 P530|||||||||
28168|Bijerkerno Metasediments|42531|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
28168|Bijerkerno Metasediments|42537|4|Described|p16|||||||||
28168|Bijerkerno Metasediments|43052|6|Mentioned|Fig.4.22|||||||||
28168|Bijerkerno Metasediments|43086|6|Mentioned|Fig.3|||||||||
28168|Bijerkerno Metasediments|43265|5|Briefly described|Map Legend||Paleoproterozoic|Of Paragon Group.||||||07-NOV-08
28168|Bijerkerno Metasediments|43266|5|Briefly described|Map Legend||Paleoproterozoic|Of Paragon Group.||||||07-NOV-08
28168|Bijerkerno Metasediments|43269|5|Briefly described|Map Legend||Paleoproterozoic|Of Paragon Group.||||||07-NOV-08
28168|Bijerkerno Metasediments|43572|6|Mentioned|Fig.3.2 p6|||||||||
28168|Bijerkerno Metasediments|46598|5|Briefly described|p305|||||||||
28168|Bijerkerno Metasediments|50045|5|Briefly described|p116 Fig. 3|Statherian|Statherian|Geological Province: Broken Hill Block. Of the Paragon Group (Willyama Supergroup). Overlain by Dalnit Bore Metasediments; underlain by Cartwrights Creek Metasediments.||||||31-MAY-07
28168|Bijerkerno Metasediments|50619|5|Briefly described|p178 Fig. 3||Paleoproterozoic|Of the Paragon Group (Willyama Supergroup).  Geological Province: Broken Hill Block.||||||07-NOV-08
28168|Bijerkerno Metasediments|60485|5|Briefly described|p28 Fig. 2|Statherian|Statherian|Marker unit.  Of the Paragon Group.  Age: <1655+/-4Ma.   Geological Province: Broken Hill Domain.||||||28-APR-05
28168|Bijerkerno Metasediments|61606|5|Briefly described|p4 Fig. 2|Paleoproterozoic|Paleoproterozoic|Of Paragon Group.||||||07-NOV-08
28168|Bijerkerno Metasediments|61735|5|Briefly described|p635 Fig. 1, 639|||Lower part of unit sampled twice and tuffaceous sediment gives depositional ages: 1657+/-4 Ma, 1655+/-4 Ma U/Pb SHRIMP.||||||04-JUN-15
28168|Bijerkerno Metasediments|61736|5|Briefly described|p666 Fig. 3|Paleoproterozoic|Paleoproterozoic|Of the Paragon Group. Ages: 1655+/-4Ma and 1657+/-4Ma. Geological province: Broken Hill Domain. Includes cream coloured, albitic, fine-grained psammites.||||||
28168|Bijerkerno Metasediments|62473|5|Briefly described|p74|||Of the Paragon Group. Age: 1656+/-5Ma. Geological province: Broken Hill Domain. Contains tuffaceous siltstones.||||||17-JUN-09
28168|Bijerkerno Metasediments|62535|5|Briefly described|p666 Fig.3, p668, p671-672, p674|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain.|1657 +/- 4 Ma; 1655 +/- 4 Ma.|Paragon Group.||Correlated with Mooleulooloo Formation.|Includes cream-coloured, albitic, fine-grained psammites.|
28168|Bijerkerno Metasediments|62536|5|Briefly described|p633, 636, 639, 641, 651-653, 655, 657|||See also p659. Broken Hill area. Depositional ages for this unit in the northern Broken Hill Block and Euriowie Block respectively.|1655 +/- 4 Ma and 1657 +/- 4 Ma (MDA).|Paragon Group.|||Tuffaceous metasiltstones, derived partly from air-fall volcaniclastic material.|
28168|Bijerkerno Metasediments|62592|5|Briefly described|p16 Fig.2.2. |||Broken Hill Domain, Curnamona Province.|<1655 +/- 4 Ma.|Unit in Paragon Group.||||
28168|Bijerkerno Metasediments|62993|6|Mentioned|p37|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain.|1655 +/- 4 Ma|Paragon Group||Overlain by Dalnit Bore Metaseidments, Overlies Cartwrights Creek Metasediments, correlated with Mooleulooloo Formation||15-DEC-21
28168|Bijerkerno Metasediments|63102|5|Briefly described|p13-14,36, p38||Neoproterozoic|Geological province: Broken Hill Domain, Curnamona Province.  Has U-Pb zircon age of 1656+\-5 Ma (Page et al. 2000).|<1655+\-4 Ma|Unit of Paragon Group.||Equivalent to Mooleulooloo Formation.||22-OCT-19
28168|Bijerkerno Metasediments|63186|5|Briefly described|p67|Paleoproterozoic|Paleoproterozoic|Of the Paragon Group (Willyama Supergroup). Geological Province: Broken Hill Domain, Curnamona Province.||||||07-NOV-08
28168|Bijerkerno Metasediments|63519|5|Briefly described|p6 Fig. 2, p10 Fig. 3|Paleoproterozoic|Paleoproterozoic|Of the Paragon Group. Overlain by Dalnit Bore Metasediments gradationally; overlies Cartwrights Creek Metasediments. Age: <1656+/-5Ma, 1660-1650Ma. Geological Province: Broken Hill Block-Euriowie Block.||||||07-NOV-08
28168|Bijerkerno Metasediments|63866|4|Described|p36, p38|Statherian|Statherian|Broken Hill Domain, Curnamona Province. Age is interpreted as the maximum depostional age for this unit.|1657 +/- 4 Ma (Page et al., 2005a)|Paragon Group||Overlies the King Gunnia Calc-Silicate Member (Cartwrights Creek Metasediments). Overlain by the Dalnit Bore Metasediments.|Thin-bedded to laminated, cross-bedded, fine feldspathic and graphitic psammite.|
28168|Bijerkerno Metasediments|64097|5|Briefly described|p302 Tb. 1, p303|Paleoproterozoic|Paleoproterozoic|Of the Paragon Group. Depositional age: 1657+/-4 , 1655+/-4Ma (Page et al 2005a).||||||07-FEB-11
28168|Bijerkerno Metasediments|64741|5|Briefly described|p301 Fig. 4|Paleoproterozoic|Paleoproterozoic|Of the Paragon Group. Age in lower section: <1655+/-4Ma. Geological province: Broken Hill Domain.||||||07-FEB-11
28168|Bijerkerno Metasediments|64742|6|Mentioned|p321 Fig.3.||||<1655 Ma.|Unit in Paragon Group.|||Psammite, psammopelite, pelite.|
28168|Bijerkerno Metasediments|64944|5|Briefly described|p26, p28 Fig. 1, , p29 Tb. 1|Paleoproterozoic|Paleoproterozoic|Of Paragon Group. Interpreted to be equivalent to the Mooeulooloo Formation in the Olary Domain. Age: <1655+/-4Ma. Geological province: Broken Hill Domain. Dating also indicates a temporal similarity with Mount Isa Group (Qld.)||||||07-FEB-11
28168|Bijerkerno Metasediments|66302|4|Described|p36 Fig.9, p38, p39, p40|Statherian|Statherian|Broken Hill Domain, Curnamona Province. |1655 +/- 4 Ma (Page et al, 2000 and Conor, 2006)|Paragon Group||Overlies the Cartwrights Creek Metasediments. Overlain by the Dalnit Bore Metasediments.|Thin-bedded to laminated, cross-bedded, fine-grained feldspathic graphitic sandstone.|
28168|Bijerkerno Metasediments|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Broken Hill Domain.|1655 +/- 4 Ma (maximum depositional age).|Paragon Group.||||
28168|Bijerkerno Metasediments|70000|5|Briefly described|p34, p37|Statherian|Statherian|||Unit in Paragon Group.||Conformably (gradationally) overlies Cartwrights Creek Metasediments.|Albitic, rippled and cross-laminated psammitic and interbedded phyllitic rocks.|
28168|Bijerkerno Metasediments|70014|5|Briefly described|Map legend|||Psammites are white to pale yellow, very fine-grained and finely laminated, with sporadic small-scale high to low angle crossbeds, flame structures, load casts, and rare graded beds. Rarely dark grey to black and lenticular.||Unit in Paragon Group.||Overlies Cartwrights Creek Metasediments. Is overlain by Dalnit Bore Metasediments.|Variably graphitic metasediments with regular, alternating psammite-rich and phyllitic intervals, 5-300m thick. Intervening phyllites are graphitic, finely laminated, spotted or non-spotted.|
28168|Bijerkerno Metasediments|70015|5|Briefly described|Map legend|Statherian|Statherian|Mineral deposits (if any) are shown.||Unit in Paragon Group.||Overlies Cartwrights Creek Metasediments.|Graphitic metapsammite and metaphyllite; the former finely laminated, with sporadic, small-scale to low-angle crossbeds, flame structures and load casts.|
28168|Bijerkerno Metasediments|70405|6|Mentioned|p9 table 1, p32, p43 Table 3|||||||Correlates with Mooleulooloo Formation||
28168|Bijerkerno Metasediments|70657|5|Briefly described|p13 Fig.6, p14-15, p43, p45|Statherian|Statherian|Curnamona Province; Broken Hill Domain.|1656 +/- 5 Ma (Page et al., 2000).|Paragon Group||Overlies Cartwrights Creek Metasediments. Underlies Dalnit Bore Metasediments. Equivalent to Mooleuloloo Formation (Olary Domain).||
28168|Bijerkerno Metasediments|70658|6|Mentioned|p15|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain, Curnamona Province.|<1655 +/- 4 Ma.|Paragon Group.||||
28168|Bijerkerno Metasediments|71968|4|Described|p18,28,45|Paleoproterozoic|Paleoproterozoic|Geological province: Curnamona province. Page et al., (2005a) reported maximum depositional ages of 1655+\-4 Ma and 1657+\-4 Ma at Broken Hill.||Unit of Paragon Group.||Overlain by Dalnit Bore Metasediments. Underlain by Cartwrights Creek Metasediments.|Thin-bedded to laminated, cross-bedded, fine feldspathic graphitic psammite.|
28168|Bijerkerno Metasediments|72461|5|Briefly described|p6, p13, p16|||Additional ages include 1655 +/- 4 Ma and 1657 +/- 4 Ma.|1656 +/- 5 Ma|Paragon Group||Overlies the Cartwrights Creek Metasediments. Overlain by the Dalnit Bore Metasediments.||
28168|Bijerkerno Metasediments|73482|5|Briefly described|p422 Fig.3, p429 Fig.8|Statherian|Statherian||1655+/-4 Ma, 1657+/-4 Ma|Paragon Group||||
28168|Bijerkerno Metasediments|73575|5|Briefly described|p828 Fig.2|Statherian|Statherian||<1655+/-4 Ma, 1657+/-4 Ma|Paragon Group||Overlies Cartwrights Creek Metasediments, underlies Dalnit Bore Metasediments||
75404|Bill's Lookout gabbro|63866|5|Briefly described|p5, p9, p31|Statherian|Statherian|Moonta Domain, Gawler Craton.|c. 1765 Ma (Johnson, 1993).|||||
75891|Billeroo Intrusive Complex|67540|2|Defined|p25; p26 Fig.1; p27-28 Tb.1,2; p37-39|Calymmian|Statherian|Formerly Billeroo North Alkaline Magmatic Complex (Rutherford et al., 2007). Type locality: 6.5 km NNW of Billeroo Hut. Curnamona Province, Western Olary Domain. Definition reference: Rutherford et al. (2007), this article and Fricke and Hore (2011). |~1610-1550 Ma|Of the Ninnerie Supersuite.||Intrudes the Ethiudna Subgroup.|Alkaline magmatic rocks. Includes massive syenite bodies, layered feldspathic ijolite phases and alkali lamprophyre dykes.|05-FEB-16
75891|Billeroo Intrusive Complex|67900|6|Mentioned|p19|||||||||
75891|Billeroo Intrusive Complex|69562|5|Briefly described|p672 Tb.5||||1610-1550 Ma (Rutherford, 2006).||||Alkaline magmatic rocks including syenite bodies, layered feldspathic ijolite phases and alkali lamprophyre dykes.|
75891|Billeroo Intrusive Complex|69650|2|Defined|p1-4, p6, p12, p16, p22, p29, p32-36|Calymmian|Statherian|See also p38, p45. Western Olary Domain, Curnamona Province. TYPE LOCALITY Significant and limited outcrop to 1 km2, approximately 6.5 km NNW of Billeroo Hut, GDA 94, 396900 mE, 6476000 mN (Fig. 11). Formerly Billeroo North alkaline magmatic complex (Rutherford et al., 2007). Limited outcrop described. Inferred age constrained by tectonic and layer-parallel fabrics. Geochemistry detailed.|c.1610-1550 Ma (Rutherford, 2006).|Unit in Ninnerie Supersuite.||Intrudes Ethiudna Subgroup.|Alkaline magmatic rocks, including massive syenite bodies, layered ijolite phases, and alkali lamprophyre dykes; associated brecciated metasediments and minor pegmatites.|25-NOV-22
75891|Billeroo Intrusive Complex|70658|5|Briefly described|p33-35|Mesoproterozoic|Paleoproterozoic|Restricted to Billeroo region, Plumbago Inlier, northern Olary Domain, Curnamona Province. Geochemistry briefly described. Limited outcrop to 1 km2.|~1610-1550 Ma.||||Alkaline magmatic rocks. Includes massive syenite bodies, layered feldspathic ijolite phases, and alkali lamprophyre dykes.|
29887|Bimba Formation|22631|4|Described|table1p172|Statherian|Statherian|||||||
29887|Bimba Formation|24431|5|Briefly described|p189 Fig. 1|||Overlies the Ethiudna Subgroup. Overlain by the Saltbush Subgroup.||||||
29887|Bimba Formation|24592|5|Briefly described|p634|||Contained within the Calc-silicate Suite of the Willyama Supergroup. Geological Province: Curnamona Province||||||
29887|Bimba Formation|43052|5|Briefly described|p86|||||||||
29887|Bimba Formation|43591|5|Briefly described|p162|||||||||
29887|Bimba Formation|50605|5|Briefly described|p9.4, 11.2|||Of the Willyama Supergroup. Geological Province: Gawler Craton and Curnamona Province. Maximum Thickness: 50m.||||||18-MAR-09
29887|Bimba Formation|60485|5|Briefly described|p28 Fig. 2|||Uppermost unit of the Curnamona Group. Lithostratigraphic equivalent of the Ettlewood Calc-Silicate Member (Broken Hill Domain).  Geological Province: Olary Domain.||||||28-APR-05
29887|Bimba Formation|61734|5|Briefly described|p52 Fig.2, p55 Fig.3 |Statherian|Statherian|A major redox boundary.||Of the Curnamona Group.||Overlies Ethiudna Subgroup. Is intruded by Basso and Lady Louise Suites. Is overlain by Saltbush Subgroup.|Metasiltstones interlayered with marble, albitic chert and calcsilicate gneiss.|
29887|Bimba Formation|61735|5|Briefly described|p658|Paleoproterozoic|Paleoproterozoic|Age: ~1693Ma. Geological province: Curnamona Province, Olary Domain. Base metal-enriched rocks.||||||
29887|Bimba Formation|61736|5|Briefly described|p664|Paleoproterozoic|Paleoproterozoic|Underlies Plumbago Formation. Min. age: 1693+/-4Ma. Base metal-enriched rocks; gossanous.||||||
29887|Bimba Formation|62514|5|Briefly described|p748 Fig. 3|Mesoproterozoic|Mesoproterozoic|||||||16-SEP-09
29887|Bimba Formation|62535|4|Described|p663-668, p670-674|Paleoproterozoic|Paleoproterozoic|Gossanous, base metal-enriched: hosts polymetallic mineralization (Zn-Pb-Ag-Cu-Co-W). Conor (2000) suggests this unit should be the uppermost in the Curnamona Group. Minimum [sic] depositional age.|>1693 +/- 4 Ma.|||Is overlain by Plumbago Formation. Equivalent to the Ettlewood Calc-Silicate Member.|Carbonate-, calc-silicate-, and sulfide-rich.|
29887|Bimba Formation|62536|5|Briefly described|p658|||Olary Domain. Overlain by a 1693 +/- 3 Ma tuffaceous metasedimentary unit, similar in age to the Broken Hill Group.|||||Calcareous and gossanous, base-metal enriched.|
29887|Bimba Formation|62592|5|Briefly described|p14, p16 Fig.2.2, p18.|||Olary Domain. Stated to be part of Broken Hill Group in text, but included as part of Curnamona Group in Fig.2.2.||Unit in Broken Hill Group.|||Pyritic, carbonate-bearing unit that is base-metal anomalous.|
29887|Bimba Formation|62993|4|Described|p3, 4, 6, 9, 11, 13-15, 18, 20, 39, 40|Paleoproterozoic|Paleoproterozoic|Olary Domain. Regional  marker horizon, although lithologically variable. See also figs on  p42, 43.|<1693 Ma|Larry Macs Subgroup||Overlain by Plumbago Formation, correlated with Ettlewood Calc-Silicate Member|40m thick quartzite overlying barite mineralisation. Biotite speckled psammopelite, discontinuous platy calc-silicate. Pyritic calcsilicates.|19-DEC-21
29887|Bimba Formation|63102|4|Described|p13-14,20,22-30,32,34-38,53-54|Statherian|Statherian|Geological province: Olary Domain, Curnamona Province. Partls interpreted as up to 200m thick. Considered to be one of two possible markers beds separating the Curnamona and Strathearn groups. Also referred to in text as Bimba suite or sulphide member. Outcrops in the Weekeroo, Billeroo, Bimbowrie and Kalabity Inliers, varying in thickness from few to few tens of meters. Contains anomalously-high base metal content (Pb-Zn-Cu-Co). Historically, Bimba Formation has been used in a variety of lithological or stratigraphic terms, and specifically poor understanding of the relationship between thin sulphidic intervals in outcropping Willyama Inliers and thick mineralised sequence below cover in Mulyungarie and Mundi-Mundi subdomains, leading to confusion (see p22-23). See also p23-26 for previously mapping attempts and facies and lithological descriptions of Bimba Formation. See p27-28 for reference localities. Possible depositional settings include: i) lacustrine/sabhka/shallow marine fine-grained organic clastic-carbonate-evaporite unit; or ii) calcareous silts and carbonate forming in an anoxic deep-water setting representing a maximum flooding surface. Contains stratiform mineralisation; laminated sulphides, associated with marble, calc-silicates and pelite - Fe Zn (Pb). Also shows stratabound mineralisation; disseminated sediment-hosted Fe, Cu, Zn, Co, W, U, F. See also ,56-60,66,68.|c. ?1705-1695 Ma|Unit of Ethiudna Subgroup.||Overlain by Plumbago Formation. Underlain by Broken Hill Group, Saltbush Subgroup, Mount Howden Group. Underlain by the Whey-Whey Formation. Equivalent to Ettlewood Calcsilicate Member.||22-OCT-19
29887|Bimba Formation|63489|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Along with unnamed equivalents of the Broken Hill Group in the Olary Domain.||||||07-NOV-08
29887|Bimba Formation|63866|4|Described|p41-p42|Statherian|Statherian|Olary Domain, Curnamona Province. Less than 50m thick. Hosts minor Pb-Zn sulphide mineralisation that is stratabound.|c. 1693 Ma|Saltbush Group||Overlain by the Plumbago Formation.|Consists of sulphidic micaceous psammite with calc-silicates and marble and contains disseminated, laminated and vein sulphides that are, at least in part, stratiform or stra-bound.|
29887|Bimba Formation|64741|4|Described|p301 Fig. 4, p309|Paleoproterozoic|Paleoproterozoic|Of Larry Macs Subgp (basal Saltbush Gp). Unconformable on Ethiudna Subgp. below. Age: <1704+/-6Ma. Geol.prov:Olary Domain.Extends into Broken Hill Domain as Ettlewood Calc-Silicate Member. See p309 for detailed description for the "Bimba-Ettlewood" unit||||||07-FEB-11
29887|Bimba Formation|64742|6|Mentioned|p321 Fig.3, P323.|||||Unit in Saltbush Subgroup.|||Calc-silicate metasediments.|29-MAR-12
29887|Bimba Formation|64944|4|Described|p26, p28 Fig. 1|Paleoproterozoic|Paleoproterozoic|Orig'ly included in Ethiudna Subgp (Curnamona Gp) in Olary Domain; then revised as basal unit of Saltbush Gp, to agree with its apparent extension into Ettlewood Calc-Silicate Mbr (Allendale Metasediments) near base of Broken Hill Gp (Broken Hill Domain).||||||07-FEB-11
29887|Bimba Formation|65925|6|Mentioned|p62.|||Metaevaporite bearing rocks.||||||
29887|Bimba Formation|66302|5|Briefly described|p36 Fig.9, p37, p39|Statherian|Statherian|Olary Domain, Curnamona Province. |1704 +/- 6 Ma|Larry Macs Subgroup||Overlain by the Plumbago Formation. Equivalent to the Ettlewood Calc-silicate Member.|Sandstone, calc-silicate and carbonate.|
29887|Bimba Formation|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Olary Domain.|1704 +/- 6 Ma (maximum depositional age).|Saltbush Group.||||
29887|Bimba Formation|67540|5|Briefly described|p31 Tb.2|||Airborne magnetics and EM data show that the Honeymoon Granite intrudes the Bimba Formation.||Of the Willyama Supergroup.||Intruded by the Honeymoon Granite.||04-FEB-16
29887|Bimba Formation|68126|5|Briefly described|p6, p29-30|Paleoproterozoic|Paleoproterozoic|Olary Domain, Curnamona Province.|<1704 +/- 6 Ma (Page et al. in prep).|Curnamona Group.||||
29887|Bimba Formation|69650|5|Briefly described|p6, p37|||||Unit in Willyama Supergroup.||Is intruded by Honeymoon Granite.|Carbonate and sulphide-rich.|
29887|Bimba Formation|70340|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic||||||Metasiltstone and metapsammite, quartz+biotite+albite+/-muscovite+/-sillimanite; calc-cilicate; marble; variably pyritic; base-metal-anomalous.|
29887|Bimba Formation|70405|4|Described|p1, p2, p9 table 1 p27, p43 Table 3, |Paleoproterozoic|Paleoproterozoic|Base metal deposits occur throughout. Also known as Bimba Suite and Bimba Sulphide Member. Lies disconformably on top of Ethiunda formation.|1693 Ma - 1700 Ma|Larry Macs Subgroup|Includes Telechie Sulphide Member|Overlies Curnamona Group, Ethiunda Subgroup, underlies Plumbago Formation, correlated with Ettlewood Calc-silicate Member|Clastic and carbonate facies interfingering. Includes medium grained quartzite, calcareous metasiltstone and calc silicate. Medium grained biotite rich psammite, coarse grained, planar bedded pure-impure marble; commonly well banded.|
29887|Bimba Formation|70657|3|Fully described|p5, p10 Fig.4, p12, p13 Fig.6, p14-16|Statherian|Statherian|See also p20-21, p24, p28-30, p32-39, p41, p43-44, p58, p60, p63-68, p73-75, p77. Curnamona Province; Olary, Mulyungarie Domains. Originally named after the Bimba Mine in the Telechie Valley. Three type areas listed; two measured sections and four reference localities detailed. Recent geochronological data force the conclusion this unit be placed in the Saltbush Group rather than the Curnamona Group, which is how it is depicted in this report. Shown as Bimba Formation + Ettlewood Calcsilicate Member in Fig.4. The base of this unit marks the base of the Curnamona Group. Thickness varies from a few centimetres to tens of metres. Significant but low-grade Zn-(Pb) mineralisation; highly prospective for Au and base metals. Lithology, gossans and skarns detailed. Ca-Fe alteration mentioned. Detrital zircon geochronology by Jagodzinski et al. (2006).|1704.9 +/-3.8 Ma (maximum deposition age).|Larry Macs Subgroup||Overlies Whey-Whey Formation, Waukaloo Formation (Ethiudna Subgroup), Portia Formation. Underlies Plumbago Formation. Correlated with Ettlewood Calc-Silicate Member.|Mixed unit of psammite, calcsilicate and carbonate. Strongly pyritic and base-metal-anomalous (Pb,Zn,Ag,W,Co,Cu). Local lone-clasts.|
29887|Bimba Formation|70658|5|Briefly described|p2-3, 5-7, 10, 15-16, 19, 25, 29, 39, 47|Paleoproterozoic|Paleoproterozoic|Olary Domain, Curnamona Province. Type section on east Ameroo Hill saddle.||Basal Larry Macs Subgroup.||Locally overlies George Mine Formation (unconformably or fault-contact). Is overlain by Plumbago Formation.|Calcic and sulfidic unit. Basal quartzite and rare pebbly psammite locally. Marble, gossan. Uppermost part is vesuvianite-bearing garnetiferous calc-silicate.|
29887|Bimba Formation|72454|6|Mentioned|p2 Fig.2|Mesoproterozoic|Mesoproterozoic|Part of Willyama Supergroup, Olary Domain.||Curnamona Group||||
29887|Bimba Formation|73021|6|Mentioned|p224|||||Broken Hill Group.||||
29887|Bimba Formation|73429|4|Described|p106 Fig.2, p107-108, p110, p111 Fig.6|Statherian|Statherian|Curnamona Province, Olary Domain. Correlated with Portia Formation, Ettlewood Calc-Silicate Member. Overlies regional unconformity and redox boundary associated with redox boundary sulfide mineralisation. Deposited in chemically reduced environment. Characterised by moderate magnetic respose metasedimentary rocks at North Portia. Location in text includes p112 Fig.7, p113.|1704+/-6 Ma maximum depositional age|base of Larry Macs Subgroup||Unconformably overlies Ethiudna Subgroup, underlies Plumbago Formation|Dominated by pyrite, marble, calc-silicate and micaceous psammite.|
69582|Bimbowrie Suite|61239|6|Mentioned|p55|||Granites, diatexite, migmatites.||||||27-MAY-06
69582|Bimbowrie Suite|62514|5|Briefly described|p746, p748 Fig. 3|Mesoproterozoic|Mesoproterozoic|Includes Bimbowrie Granite.  S-type granitoids and associated pegmatites. Age: <1600Ma. Geological Province: Olary Domain/Curnamona Province.||||||16-SEP-09
69582|Bimbowrie Suite|62592|5|Briefly described|p16 Fig.2.2, p18 .|Calymmian|Statherian|Olary Domain, Curnamona Province. S-type. Coeval with 1580 Ma Benagerie Volcanics.|c.1600-1580 Ma.|Unit in Ninnerie Supersuite.|||Muscovite + biotite granite.|
69582|Bimbowrie Suite|62724|5|Briefly described|p20|Mesoproterozoic|Mesoproterozoic|See also Bimbowrie Suite granite.||||||07-FEB-11
69582|Bimbowrie Suite|62993|5|Briefly described|p5, 16, 24, 25, 31, 42-44|Mesoproterozoic|Mesoproterozoic|||Ninnerie Supersuite||Intrudes Willyama Supergroup|S-type, biotite-muscovite granites.|19-DEC-21
69582|Bimbowrie Suite|63020|5|Briefly described|p987 Fig. 8|Mesoproterozoic|Mesoproterozoic|Age: 1590Ma. Geological Province: Curnamona Province (Olary Domain).||||||10-AUG-07
69582|Bimbowrie Suite|63102|5|Briefly described|p41,63|Calymmian|Calymmian|Geological province: Olary Domain, Curnamona Province. See Bimbowrie Supersuite. |1580 Ma|||Intrudes into Ethiudna Subgroup.|Syenite, ijolite, minor possible carbonatite (calcite and siderite), and breccia.|
69582|Bimbowrie Suite|63224|6|Mentioned|p12|||Geological Province: Curnamona Province.||||||07-FEB-08
69582|Bimbowrie Suite|63866|5|Briefly described|p42||||1581 +/- 3 Ma (Page et al., 2005b)|Ninnerie Supersuite|||S-type granites.|
69582|Bimbowrie Suite|64316|6|Mentioned|p534|||Stated to be a 'former term' for Olary regional S-type granitoids of Ashley et al (1996) but superseding name, if any, is not given.||||||07-FEB-11
69582|Bimbowrie Suite|64741|5|Briefly described|p313|||Of the Ninnerie Supersuite (1590-1580Ma). Dominantly potassic S-type two-mica granites.||||||07-FEB-11
69582|Bimbowrie Suite|65220|6|Mentioned|p19 Fig.1|Mesoproterozoic|Mesoproterozoic|||||||10-DEC-09
69582|Bimbowrie Suite|65376|6|Mentioned|p9 Fig.1.2. |Mesoproterozoic|Mesoproterozoic|||||||
69582|Bimbowrie Suite|65455|6|Mentioned|p9 Fig. 5|||Curnamona Province. Exhibits elevated U contents.|||Includes Crockers Well Granite.|||09-MAY-12
69582|Bimbowrie Suite|66302|5|Briefly described|p50, p51|||Olary Domain, Curnamona Province. Ages derived from Cook et al. (1994) and Page et al. (2005).|1592 to 1580 Ma |Ninnerie Supersuite|||Potassic, S-type, biotite/muscovite granites.|
69582|Bimbowrie Suite|66522|6|Mentioned|p28.|Proterozoic|Proterozoic|Curnamona Province. Likely source of zircons of this age found in Kooringa Member.|c.1590 Ma.|||||
69582|Bimbowrie Suite|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Olary Domain.|1592 +/- 3 Ma to 1581 +/- 3 Ma.|||||
69582|Bimbowrie Suite|67536|5|Briefly described|Map Legend|Calymmian|Statherian|Curnamona Province. Informally subdivided into two parts: silicic intrusives (M36), and mafic equivalents (M37).|ca. 1616 +/- 9 Ma - 1579 +/- 2 Ma||||Mainly S-type monzogranite, quartz monzodiorite, granodiorite and sodic granitoids; mafic intrusive equivalents.|
69582|Bimbowrie Suite|67540|4|Described|pp25-28, p36 Tb.3, p37, p38 Fig.2|Calymmian|Calymmian|Regional granites of Ashley, Conor and Skirrow (1998); 'Bimbowrie Granites' of Benton (1994); 'Bimbowrie Suite' of Conor (2004). Type locality occurs at Triangle Hill. Definition reference: this article and Fricke and Hore (2011). Curnamona Province, Olary Domain. Ages from Jagodzinski and Fricke (2010), and Page et al. in prep., respectively.|1594+/-8 Ma (SHRIMP II)-1581+/-3 Ma(U-Pb zircon)|Of the Ninnerie Supersuite.|Includes Triangle Hill Granite, Binberrie Hill Granite, 'Mundaerno Granite'.|Intrudes Willyama Supergroup.|Medium- to coarse-grained, massive to foliated, equigranular to strongly porphyritic muscovite-biotite monzogranites; variably magnetic.|
69582|Bimbowrie Suite|67621|6|Mentioned|p224|||Curnamona Province.||||||
69582|Bimbowrie Suite|67653|4|Described|p3-4|Calymmian|Calymmian|Geological province: Curnamona Province. Emplacement date from Fricke 2008. Crops out in the Olary Domain. Diffuse contacts with the surrounding metasediments, which together with Nd isotopic constraints suggests that it was derived via melting of surrounding Willyama Supergroup metasedimentary rocks (Barovich and Ashley, 2002; Fricke, 2008).|~1592-1580 Ma|||||
69582|Bimbowrie Suite|67900|6|Mentioned|p19|||Curnamona Province.||Ninnerie Supersuite.|||Muscovite-biotite granites.|
69582|Bimbowrie Suite|68067|6|Mentioned|Map legend.|||Areas with higher magnetic response are mapped separately.||||||27-AUG-13
69582|Bimbowrie Suite|68126|5|Briefly described|p3, p5-7|||Olary Domain, Curnamona Province. Several age determinations listed in the range ~1580-1592 Ma.|1592+/-3 Ma; 1581+/-3 Ma (Page et al. in prep).|Ninnerie Supersuite.|||Muscovite-biotite, regional granites.|
69582|Bimbowrie Suite|68131|5|Briefly described|p2 Fig.1|Mesoproterozoic|Mesoproterozoic|Mapped with Hiltaba and Moolawatana Suites as a single unit.|||||Granitic rocks and felsic porphyry.|
69582|Bimbowrie Suite|68715|6|Mentioned|p32 Fig.6||||||||Granitoids.|07-APR-17
69582|Bimbowrie Suite|69019|5|Briefly described|p29 Fig.9.|||Olary Province. Appears as Bimbowrie Suite Granite, and also mis-spelt as Bimbowie, in Fig.9. Geochemistry is briefly described.|||||Muscovite granite.|
69582|Bimbowrie Suite|69023|5|Briefly described|p26|||Olary Province. Geochemistry outlined.|||||Includes muscovite granite.|
69582|Bimbowrie Suite|69213|5|Briefly described|p34|Paleoproterozoic|Paleoproterozoic|Curnamona Province. May be derived from partial melting of Willyama Supergoup.|||||Coarse grained, two mica, S-type mainly potassic granites. Some deformation where they are cut by retrograde shear zones; granitic dykes.|
69582|Bimbowrie Suite|69562|5|Briefly described|p671 Tb.5, p674 Fig.6||||1581 +/- 3 Ma (Jagodzinski & Fricke, 2010).|Unit in Ninnerie Supersuite.|||Medium- to coarse-grained muscovite-biotite granite characterised by large K-feldspar phenocrysts.|
69582|Bimbowrie Suite|69650|2|Defined|p4 Tb.1, p2, p5 Tb.2, p10 Tb.3, p12|Calymmian|Calymmian|See also p15-20, p22, p28-29, p34, p37-38, p41, p45. Olary Domain, Curnamona Province. Named after Bimbowrie Homestead, 29 km NW of Olary. Previously Bimbowrie Granites (Benton, 1994); later Bimbowrie Granite, and Bimbowrie Suite (Conor, 2000). Type locality Triangle Hill, GDA 94, zone 54, 428214 mE, 6460831 mN (Fig. 2) and Binberrie Hill. Broad, diffuse migmatitic aureoles within host Willyama Supergroup metasediments. Geochronology results, geochemistry detailed.|1594-1580 Ma.|Unit in Ninnerie Supersuite.|Includes Binberrie Hill, Triangle Hill, Mundaerno Granites.||Medium- to coarse-grained, massive to foliated, equigranular to strongly porphyritic muscovite-biotite monzogranites; variably magnetic. S-type (some I-type).|25-NOV-22
69582|Bimbowrie Suite|69654|5|Briefly described|p3, 21-23|Mesoproterozoic|Mesoproterozoic|Curnamona Province. Granites were derived from partial melting of Willyama Supergroup metasediments.|~1590 Ma.|Ninnerie Supersuite.|||Consists of two-mica S-type granites.|
69582|Bimbowrie Suite|70340|5|Briefly described|map legend|Mesoproterozoic|Mesoproterozoic||U-Pb age 1592-1580 Ma||||Monzogranite, biotite-muscovite.|
69582|Bimbowrie Suite|70405|4|Described|p1, p46, p97|Mesoproterozoic|Mesoproterozoic||1590 Ma -1580 Ma|Ninnerie Supersuite|||Muscovite-biotite K feldspar granites and quartz monzonites with S Type affinities. Undeformed except where cut by narrow, late greenschist facies shear zones.|
69582|Bimbowrie Suite|70657|5|Briefly described|p48-49, p69|Calymmian|Calymmian|Olary Domain, Curnamona Province. Originally the Bimbowrie Granites (Benton, 1994). Modified by Conor (2000) to Bimbowrie Suite, and later (Conor, 2004) to Bimbowrie Supersuite. Proposed in this study to discontinue the name Bimbowrie Supersuite, to restrict the Bimbowrie Suite to include the "regional" two-mica S-type granites (outside the Crocker Well - Billeroo area), and to introduce the new name Ninnerie Supersuite to include all Mesoproterozoic granites in the region. Numerous ages (mostly SHRIMP) given.|1592 +/- 3 Ma - 1581 +/- 3 Ma.|||||
69582|Bimbowrie Suite|70658|5|Briefly described|p29, 33-34, 36|Mesoproterozoic|Mesoproterozoic|Olary Domain, Curnamona Province. Geochemistry briefly described.|1594-1580 Ma.|Ninnerie Supersuite.|||Medium- to coarse-grained, massive to foliated, equigranular to strongly porphyritic peraluminous (S-type) muscovite-biotite monzogranites. Variably magnetic.|
69582|Bimbowrie Suite|70659|6|Mentioned|p3 fig 1|||Curnamona Province.||||||
69582|Bimbowrie Suite|72454|5|Briefly described|p2-3, 7-12, 17-26, 28-30, 32-35, 39-40,|Calymmian|Calymmian|Part of the Olary Domain. Oldest interpreted magmatic age 1592+/-3 Ma (Page 2005). Youngest magmatic age from granite collected from Rock Wallaby Creek with U-Pb zircon age of 1581+/-3 Ma Page (2005). Bimbowrie Suite granites were largely derived from melting of Willyama Supergroup sediments. See also p42, 44, 46-49, 51-59, 81-82. Granitic rocks of this suite are variably magnetic, strongly peraluminous with S-type affinities, though not typical S-type of White and Chappell as garnet and cordeirite are absent.|1592+/-3 to 1581+/-3 Ma.|Ninnerie Supersuite||Coeval with Crocker Well Suite.|Includes sodic to biotite only granites and granodiorites to diorites and poryritic granitoids. Two mica granites are pink or buff to cream, medium-coarse-grained, massive to foliated, equigranular to porphyritic and leucocratic.|22-MAY-21
69582|Bimbowrie Suite|72949|6|Mentioned|p35-36|Calymmian|Calymmian|Curnamona Province. Broken Hill / Olary Blocks.|1594-1580 Ma|||||
69582|Bimbowrie Suite|73030|6|Mentioned|p2149|Calymmian|Calymmian|Curnamona Province.||||||
69582|Bimbowrie Suite|73165|6|Mentioned|p637, Fig. 12|||Curnamona Province.||||||
75893|Binberrie Hill Granite|67540|3|Fully described|p25, p27 Tb.1, p28 Tb.2|Calymmian|Calymmian|Type locality: Binberrie Hill, 23 km N of Olary. Curnamona Province: Olary Domain. Geochemistry outlined. S-type. Definition reference: this article and Fricke and Hore (2011).|~1580 Ma|Of the Bimbowrie Suite.||Intrudes the Willyama Supergroup.|White, cream to pink, coarse-grained, equigranular muscovite-biotite monzogranites; variably magnetic.|08-FEB-16
75893|Binberrie Hill Granite|69650|2|Defined|p4 Tb.1, p5 Tb.2, p12, p16, p19-20|Calymmian|Calymmian|New name, TYPE LOCALITY: Significant outcrop at Binberrie Hill, GDA 94, zone 54, 435555 mE, 6451045 mN, after Binberrie Hill, 23 km N of Olary. Previously part of Bimbowrie Granites. Commonly has broad, diffuse migmatitic aureoles within host Willyama Supergroup metasediments. Geochemistry outlined.  SHRIMP U-Pb zircon age.|c.1580 Ma; Cook et al., (1994).|Unit in Bimbowrie Suite.|||White, cream to pink, coarse-grained, equigranular, muscovite-biotite monzogranites; variably magnetic. S-type.|25-NOV-22
75893|Binberrie Hill Granite|70658|5|Briefly described|p33-34, 36|Mesoproterozoic|Mesoproterozoic|Olary Domain, Curnamona Province. Geochemistry briefly described. Large domal outcrops.|c.1580 Ma.|Bimbowrie Suite.|||White, cream to pink, coarse-grained, equigranular muscovite-biotite monzogranites; variably magnetic.|
29906|Birksgate Complex|23483|5|Briefly described|p4|||||||||
29906|Birksgate Complex|24197|5|Briefly described|p97, p98|||Refers to all metamorphic rocks (granulites and amphibolite-facies gneisses) south of Woodroffe Thrust (Fregon Domain) - excl.Giles Complex and Kulgera Supersuite. Includes Wataru Gneiss. Comprises >90% acid lithologies. Geol. Province: Musgrave Block.||||||07-FEB-11
29906|Birksgate Complex|24496|4|Described|p14|Mesoproterozoic|Mesoproterozoic|Includes massive orthogneiss and well layered gneisses, and migmatites. Volcanosedimentary protoliths with ages: ~1550 and ~1300 Ma. Unconformably overlain by Bentley Supergroup. Geological Province: Musgrave Block.||||||03-AUG-09
29906|Birksgate Complex|24497|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Geological Province: Musgrave Block.||||||
29906|Birksgate Complex|24499|5|Briefly described|Map legend|||Of the Bentley Supergroup?||||||
29906|Birksgate Complex|43052|5|Briefly described|p158|||||||||
29906|Birksgate Complex|43053|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Metasediments, gneiss, granulite. Includes Wataru Gneiss. Geological Province: Musgrave Block.||||||07-NOV-08
29906|Birksgate Complex|43258|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
29906|Birksgate Complex|43298|6|Mentioned|Map Legend||Paleoproterozoic|||||||07-NOV-08
29906|Birksgate Complex|43561|6|Mentioned|p1439|||||||||
29906|Birksgate Complex|50607|6|Mentioned|p1.1|||Geological Province: Musgrave Block. Intruded by: Kulgera Supersuite, Winburn Suite.||||||
29906|Birksgate Complex|60660|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Includes granulite, gneiss, migmatite and granite. Geological Province: Musgrave Block.||||||22-FEB-05
29906|Birksgate Complex|60662|5|Briefly described|Map Legend|||Includes layered granulites.||||||22-FEB-05
29906|Birksgate Complex|60953|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Age: ~1560-1300Ma. Granulite to amphibolite facies quartzofeldspathic gneiss, felsic to ultramafic orthogneiss, peltic-calcic paragneiss and iron formation.||||||
29906|Birksgate Complex|61108|5|Briefly described|map legend|Mesoproterozoic|Mesoproterozoic|Granulite to amphibolite facies quartzofeldspathic gneiss, felsic to ultramafic orthogneiss, pelitic-calcic paragneiss and iron formation. Age: ~1560-1300 Ma.||||||
29906|Birksgate Complex|61524|5|Briefly described|p16|Mesoproterozoic|Mesoproterozoic|Leucocratic quartz-feldspar gneiss, felsic granulite gneiss and melanocratic quartz-hypersthene gneiss. Age: ~1600-1300 Ma. Geological Province: Musgrave Province. See also p17 Fig.1, p18 Fig. 2(a)||||||
29906|Birksgate Complex|61864|5|Briefly described|p18, p19 fig 5|||Part of the basement of Musgrave Province. Sediments and volcanics.|||||Granulite to amphibolite-facies gneiss: para- and orthogneisses with interlayered mafic gneiss.|
29906|Birksgate Complex|64645|5|Briefly described|p16 Fig. 2|Mesoproterozoic|Paleoproterozoic|Age: 1600-1300Ma. Geological Province: Musgrave Province.||||||
29906|Birksgate Complex|64722|5|Briefly described|Fig. 2 p3-6, p16|Calymmian|Calymmian|Oldest exposed unit in Musgrave Orogen. Contains 1600-1500 Ma zircons. Geochemistry suggests subduction related environment to 1555 Ma.|||||Comprises felsic rocks, subordinate mafic units, rare metapelite, quartzite, calcsilicate rock.|11-APR-12
29906|Birksgate Complex|64745|5|Briefly described|p372, p373 Fig. 3, p374 Tab. 1|||Included within informal Musgravian Gneiss in this paper. Geol. Prov: Fregon Domain, Musgrave Province.||||||
29906|Birksgate Complex|64831|5|Briefly described|p1128 Fig. 2|Mesoproterozoic|Mesoproterozoic|Age: ca 1590-1550Ma. Comprises felsic, intermediate and mafic gneisses - dominantly felsic orthogneiss with subordinate mafic gneiss, intermediate gneiss and metasedimentary rocks. See also p1131.||||||
29906|Birksgate Complex|65135|6|Mentioned|p5|||Used to describe all rocks deformed during the Musgravian Orogeny by Major and Conor (1993)||||||
29906|Birksgate Complex|65376|6|Mentioned|p9 Fig.1.2. |Mesoproterozoic|Mesoproterozoic||||||Metasedimentary and meta-igneous gneiss.|
29906|Birksgate Complex|65385|5|Briefly described|pS132|Calymmian|Calymmian|~1600-1400 Ma. Intruded by Pitjantjatjara Supersuite.||||||08-MAR-12
29906|Birksgate Complex|65833|6|Mentioned|p5.|||Musgrave area. Of Major and Conor (1993), who included all rocks formed prior to, and metamorphosed during, the 1225-1150 Ma Musgravian Orogeny.||||||
29906|Birksgate Complex|65906|5|Briefly described|p5|Mesoproterozoic|Mesoproterozoic|Large proportion of outcrop in Musgrave Block. Gneisses deposited between 1600-1540 Ma as sedimentary rocks, with volcanics and volcaniclastics. Felsic; island-arc subduction affinities.||||||
29906|Birksgate Complex|67128|6|Mentioned|p6-7|||Includes all gneisses in the eastern Musgrave Province. Some of these were thought to have granitic protoliths up to 1590 +/- 25 Ma old; these now appear to be due to detrital zircon components.||||||
29906|Birksgate Complex|67323|6|Mentioned|Eastern Australia Time-Space Plot|||Musgrave Block.||||||
29906|Birksgate Complex|67375|5|Briefly described|p6, p17. |||Musgrave Province. Included all rocks metamorphosed during the Musgrave Orogeny, including the Mesoproterozoic granite suites and the basement they intruded.||||||
29906|Birksgate Complex|67536|5|Briefly described|Map Legend|||Musgrave Block. Informally subdivided into four parts, one of which is demagnetised or altered gneiss or granulite adjacent to major structures or Giles Complex intrusives. Non-magnetic, weakly magnetic, moderately magnetic, and variably magnetic in parts.|||Includes Wataru Gneiss.||Sheared, altered or granite-intruded gneiss or granulite adjacent to major shear zones; massive mainly meta-igneous gneiss and granulite, may include charnockite/migmatite alteration of layered granulite; layered metasedimentary gneiss and granulite.|02-APR-14
29906|Birksgate Complex|67921|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Shown only in section.|||||Metasediments, gneiss, granulite.|
29906|Birksgate Complex|68100|6|Mentioned|p4, 6 |||Of Major and Conor (1993). Fregon Domain. Includes gneissic basement rocks. Gneissic rocks called Wirku Metamorphics in west Musgrave Province.||||||19-JAN-17
29906|Birksgate Complex|68131|5|Briefly described|p2 Fig.1|Mesoproterozoic|Mesoproterozoic||||||Metasedimentary and meta-igneous gneiss.|
29906|Birksgate Complex|69091|6|Mentioned|p60, p103 Fig.5.6|||In South Australian section of Musgrave Province, all rocks metamorphosed during Musgrave Orogeny, including Mesoproterozoic granite suites and basement through which they intruded, were initially grouped into Birksgate Complex (Major and Conor, 1993). However, recent work has shown that much of what was previously regarded as exposed basement in west Musgrave Province actually comprises supracrustal packages (now mainly paragneiss) deposited between c. 1340 Ma and 1270 Ma (Evins et al., 2012) - referred to as Wirku Metamorphics (Howard et al., 2007; Evins et al., 2009; Smithies et al., 2009).||||||
29906|Birksgate Complex|69213|5|Briefly described|p35, p36 Fig. 12, p28-29 fig.6|||Musgrave Province.|||||Gneisses. Stromatic metatexite migmatite defined by layer parallel, mostly in source leucosomes. Leucosomes of two types; medium grained, straight margined and coarse grained less sharp margined leucosomes.|
29906|Birksgate Complex|69436|6|Mentioned|p21:2-3||||1600-1540 Ma.|||||12-JUL-16
29906|Birksgate Complex|69640|4|Described|p11-p14, p16-p17, p24, p31-p32|Proterozoic|Proterozoic|Musgrave Province. Subsequently deformed and metamorphosed to amphibolite to granulite facies during the ca 1220-1120 Musgrave Orogeny. Petrology, petrographic description, SHRIMP methodology, results and analayses for numerous samples are provided. An additional magmatic crystallisation age of 1617 +/- 8 Ma was obtained. A maximum depositional age of 1588 +/- 7 Ma was also obtained for a quartzo-feldspathic gneiss. Metamorphic ages inculding 1158 +/- 8 Ma are provided. See also p50, p57, p65, p73-p74, p79, p137, p141, p145, p157.|1605 +/- 6 Ma (SHRIMP, magmatic crystallisation)|||Intruded by the Pitjantjatjara Supersuite.|Felsic ortho- and paragneisses including biotite quartzo-feldspathic paragneiss, hornblende-biotite-diopside quartzo-feldspathic gneiss, migmatitic gneiss.|
29906|Birksgate Complex|69729|5|Briefly described|p67, p88|||Major and Conor (1993), for west Musgrave Province basement defined as rock metamorphosed during the Musgrave Orogeny. These were reassigned (Howard et al., 2009) to Wirku Metamorphics on the basis of geochronology (discussed).||||||
29906|Birksgate Complex|70083|5|Briefly described|p206-208, 229|||The name used for the Musgravian Gneiss in the Fregon Subdomain, Eastern Musgrave Inlier, Musgrave-Albany-Fraser Orogen. Is termed the Olia Gneiss in the Mulga Park Subdomain.|||Kalamurta Gneissic Unit.|Is dissected (intruded) by Alcurra Dolerite dykes.|Peraluminous metapelite gneiss, intercalated with more quartzofeldspathic, and granitic gneisses.|12-MAY-23
29906|Birksgate Complex|70338|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Part of the basement to the Musgrave Province. The five facies are mapped separately.|||||Gneiss, granulite and amphibolite facies S of the Woodroffe Thrust. Pale brown, quartzo-feldspathic granofels; layered, quartzo-feldspathic orthogneiss to leucogneiss; layered to migmatitic, quartzo-feldspathic paragneiss; meta-calcsilicate rock.|
29906|Birksgate Complex|70634|6|Mentioned|189540.1.pdf|||Now named Wirku Metamorphics.||||||
29906|Birksgate Complex|71170|5|Briefly described|p9, p23|||Musgrave Province. Name derived from Major and Conor, 1993.||||||
29906|Birksgate Complex|71321|4|Described|p1-2,4-5,8,14,17-18,21,24|Calymmian|Statherian|Geological province: Musgrave Province. Comprises part of basement, and oldest rocks exposed on the Musgrave Province. Occurs in outcrop as blocks or rafts (several cm to hundreds of meters across) within Pintjantjatjara Supersuite. See p14-17 for detailed descriptions of outcrop. Deformed (early gneissic layering and folding) and metamorphosed to amphibolite to granulite facies during c. 1220-1120 Ma Musgravian Orogeny. Intruded by granitoid bodies of Pintjantjatjara Supersuite. Geochemically similar to c. 1345-1293 Ma Wankanki Supersuite granites in the West Musgrave Province (strong compositional similarities to Phanerozoic granites of the Andean continental arc (Smithies, et al., 2010). Dominantly metaluminous, to slightly peraluminous and predominantly magnesian character; strong affinity to I-type granites. Likely formed in a volcanic arc setting. Has c. 1620-1550 Ma zircons indicating igneous protolith age (Camacho and Fanning, 1995; Edgoose, et al., 1993; Edgoose, et al., 2004; Scrimgeour, et al., 1999); protolith magmatic ages as early as c. 1665 Ma from adjacent AGNES CREEK mapsheet. Emplacement ages in the HANGING KNOLL map include c. 1480 Ma and c. 1440 Ma. Nd and Hf isotopic analysis indicate a relatively juvenile source for both para- and orthogneisses. Considered prospective for Zn-Pb-Ag ore bodies similar to Broken Hill. See also p32-41,55-56,60-63,66-67,74.|c. 1630-1560 Ma||||Felsic and mafic orthogneisses and felsic volcanics, volcaniclastics and paragneisses.|
29906|Birksgate Complex|71322|5|Briefly described|p11-19, p26, p28|||Musgrave Province. Hosts Cu mineralisation at the Kenmore II prospect. Summary log for drillhole DD10WOD007. Leococratic migmatite dated. Metamorphosed at 1180 +/- 5 Ma and 1159 +/- 7 Ma.|1520 +/- 9 Ma (maximum depositional age).||||Intermediate to felsic migmatitic gneisses, paragneisses, orthogneisses and intrusive magmatic rocks, calcsilicate, schist.|13-DEC-21
29906|Birksgate Complex|71416|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|The six facies are mapped separately. Most have protolith ages given. Metamorphosed between c.1170 Ma and 1138 Ma. Solid geology interpretation: demagnetised or altered adjacent to major structures or Giles Complex intrusives; non-magnetic, weakly or variably magnetic.|c.1716 Ma - 1565 Ma.|||Correlative of Kalamurta gneiss.|Quartzo-feldspathic paragneiss, commonly migmatitic; mixed felsic +/- mafic gneiss; amphibolite to granulite facies felsic gneiss, commonly migmatitic; leucocratic diatexite; mafic gneiss, locally migmatitic; undivided gneiss, locally migmatitic.|
29906|Birksgate Complex|71536|6|Mentioned|p73, p78|||Was likely the protolith of the 1143 +/- 9 Ma felsic gneiss in the Pitjantjatjara Supersuite.||||||
29906|Birksgate Complex|71592|5|Briefly described|Appendix A.|||Musgrave Province. Over 20 age determinations are given for crystallisation (within this range), provenance clusters and metamorphism.|1617+/-8 Ma to 1564+/-5 Ma.||||Gneiss, syenogranitic gneiss, granite, monzogranite, pelitic to semipelitic migmatite.|
29906|Birksgate Complex|72238|5|Briefly described|p38|Calymmian|Statherian|Geological province: Musgrave Province. Intruded by Amata Dolerite.|c. 1.7-1.5 Ga|||||
29906|Birksgate Complex|72242|6|Mentioned|p27|Calymmian|Statherian|Geological province: Musgrave Province. Associated with Kararan Orogeny. Coeval with Hiltaba Suite and Toolgana Supersuite, and extensive oceanic crust formation.||||||
29906|Birksgate Complex|72344|6|Mentioned|p28|Calymmian|Statherian|Musgrave Province.|c. 1565-1665 Ma (Jagodzinski et al, 2013)|||Time equivalent to the Toolgana Supersuite.||
29906|Birksgate Complex|72476|5|Briefly described|p24, 27|||Dominant basement unit in eastern Musgrave Province.|~1650-1550 Ma.||||Granulite to upper amphibolite facies, volcanic-dominated supracrustal rocks and felsic intrusives (granites through to tonalites, minor intercalated mafics), with minor sedimentary rocks.|
29906|Birksgate Complex|73100|5|Briefly described|Map legend|Palaeoproterozoic|Palaeoproterozoic|Subsurface.|||||Metasediments, gneiss, granulite.|
29906|Birksgate Complex|73109|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Drexel et al. (1993). Subsurface.|||||Metasediments, gneiss, granulite.|
29906|Birksgate Complex|73111|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Subsurface.|||||Metasediments, gneiss, granulite.|
29906|Birksgate Complex|73232|6|Mentioned|p5|||Musgrave Province. This unit dominates the province.||||Intruded by Pitjantjatjara Supersuite and Giles Complex including Alcurra Dolerite.|Deformed and metamorphosed gneissic rocks.|
29906|Birksgate Complex|73234|6|Mentioned|p19|Calymmian|Statherian|Musgrave Province, eastern.|c. 1700-1550 Ma||||Meta-igneous and metasedimentary rocks.|
23390|Bittali Rhyolite|40430|2|Defined|p6|Mesoproterozoic|Mesoproterozoic|||||||
23390|Bittali Rhyolite|41619|6|Mentioned|Map legend|Mesoproterozoic||||||||
23390|Bittali Rhyolite|42466|5|Briefly described|Map Legend|||||||||
23390|Bittali Rhyolite|42475|4|Described|p16|||part of "older" Gawler Range Volcanics||||||
23390|Bittali Rhyolite|42546|5|Briefly described|Map legend|Mesoproterozoic||||||||
23390|Bittali Rhyolite|42736|5|Briefly described|map legend|Mesoproterozoic||||||||
23390|Bittali Rhyolite|43052|5|Briefly described|p109|||of Gawler Range Volcanics||||||
23390|Bittali Rhyolite|65221|5|Briefly described|p28 Fig.3a |Mesoproterozoic|Mesoproterozoic|Of Gawler Range Volcanics||||||
23390|Bittali Rhyolite|65922|5|Briefly described|p16, p17 Tb. 2, p18|Calymmian|Calymmian|Upper unit of the 'older' or 'lower' Gawler Range Volcanics. Yellowish brown to cream rhyolite and rhyodacite lavas, lava domes, welded ash flows and feeder dykes; aphanitic, eutaxitic or porphyritic. Conformably overlies Waganny Dacite; overlies Lincoln Complex and Warrow Quartzite. Conformably underlies Nonning Rhyodacite and Eucarro Dacite.||||||
23390|Bittali Rhyolite|67028|5|Briefly described|p362, p364 Tb.1|Calymmian|Calymmian|Information on magnetic characteristics presented. Described as Roxby Downs-type p362, but shown as Kokatha-type in Table 1.||Gawler Range Volcanics||||24-APR-12
23390|Bittali Rhyolite|68158|6|Mentioned|p4|||||Gawler Range Volcanics.|||Rhyolite to rhyodacite crystal and lithic-lapilli ash flow tuffs, air-fall tuffs and lava-flows; massive porphyritic rhyolite.|
23390|Bittali Rhyolite|70659|5|Briefly described|p5-8, p43|Mesoproterozoic|Mesoproterozoic|SW and S margins of the Gawler Ranges. Appears as Bitalli Rhyolite on p6 and p8.||Lower Gawler Range Volcanics.||Overlies Waganny Dacite.|Quartz-phyric rhyolite to rhyodacite lava flows, ignimbrites, polymict breccia, lava domes, feeder dykes and crystal-rich and pumiceous tuffs.|
23390|Bittali Rhyolite|70816|5|Briefly described|p4-5,19|||SW and S Gawler Ranges margin.||Unit of lower Gawler Range Volcanics.||Underlain by Waganny Dacite.|Rhyolitic lavas, ignimbrite and tuff|
23390|Bittali Rhyolite|71317|4|Described|p1, p20-p26, p54, p58|Mesoproterozoic|Calymmian|Gawler Craton. Has a lateral extent of over 200km and comprises three distinct volcanic successions; these are briefly described. A detailed lithology is provided for the Peltabinna map area. Estimated thickness at its type locality at Bittali Dam is 200m. Age provided is a U-Pb CA-TIMS age of a sample from Wataka 150km east of Peltabinna. See also p96, p114, p150, p170, p176.|1589.3 +/- 5 Ma (Jagodzinski et al., 2016)|Gawler Range Volcanics||Overlain by the Eucarro Rhyolite.|Porphyritic feldspar- and quartz-phyric rhyolite lava which has a flow-banded and amygdaloidal top and locally contains granitoid xenoliths.|
23390|Bittali Rhyolite|71418|6|Mentioned|p21|Mesoproterozoic|Mesoproterozoic|Geological province: Gawler Craton.||||||
23390|Bittali Rhyolite|71559|4|Described|p16, p19-20, p22|Mesoproterozoic|Mesoproterozoic|Geological province: Gawler Craton.||Unit of Lower Gawler Range Volcanics.|||Rhyolitic to rhyodacitic aphyric to quartz-phyric lavas and ignimbrites and rhyolitic feeder dykes.|19-JUN-19
23390|Bittali Rhyolite|71560|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|||Lower Gawler Range Volcanics.|||Rhyolitic to rhyodacitic, aphyric to quartz- and feldspar-phyric lavas and ignimbrites and rhyolitic feeder dykes.|
23390|Bittali Rhyolite|72090|4|Described|p12, p15, p67-p68, p98, p101|||Gawler Craton. Intruded by an unnamed porphyritic dacite dyke near Peterlumbo Hill. Misspelt as the Bitalli Rhyolite on p12. Intersected in drillhole MSDP10. The top of this unit is intensely sericite altered. Additional samples are described.|1588.5 +/- 0.5 Ma|Gawler Range Volcanics, Lower||Overlies the Eucarro Rhyolite.|Yellowish grey, sericitic, monomict quartz-phyric rhyolite breccia. Greenish grey, pervasive quartz-sericite-pyrite, quartz-phyric, flow-banded rhyolitic lava.|
23390|Bittali Rhyolite|72459|5|Briefly described|p17, p46|Mesoproterozoic|Mesoproterozoic|Occurs near the Bittali Dam north of Buckleboo in the Coulta/Cleve subdomain. Outcrops are isolated and interpreted to belong to the developmental phase of the Gawler Range Volcanism.||Gawler Range Volcanics||||
23390|Bittali Rhyolite|72464|5|Briefly described|p2, 8|Mesoproterozoic|Mesoproterozoic|Gawler Craton.||||Is intruded by dacite of the Gawler Range Volcanics.||
23390|Bittali Rhyolite|73104|6|Mentioned|p3|Mesoproterozoic|Mesoproterozoic|||||||
23390|Bittali Rhyolite|73110|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|||Lower Gawler Range Volcanics.|||Rhyolite-rhyodacite, feeder dykes and welded ash.|
23390|Bittali Rhyolite|73162|6|Mentioned|p459|||In Wartaka area 40km WNW of Roopena Basin. Possible source of tuffs in Fresh Well Formation.|||||Succession of felsic tuffs and lavas.|
73421|Bittles Tank Volcanics|66623|2|Defined|p74, 80, pp95-97, p229.|Middle Cambrian|Middle Cambrian|Defined as an igneous suite in this study. Formerly part of Wonominta beds (Warris 1967), unit in Ponto beds (Mills 1992), in Ponto Group (Stevens et al. 2000). Tholeiitic magmatism which continued late into the Delamerian Orogeny, with numerous small, scattered gabbro plutons. Deeper water environment. Type locality at Benny Hill, Kayrunnera Station. Has age and geochemical correlations with Glenelg Complex.|c.510 Ma (Black 2006) to 496.3 +/- 3.1 Ma.|Unit in Ponto Group.|No formal members; includes previously (Buckley 2000) reserved Ponto Group members including Blue Rock Well, Gum Creek and Tekum Creek Basalts; informal Kayrunnera Gabbro and Nuntherungie Dolerite.|Intrudes Teltawongee, Grey Range and Ponto Groups. Is unconformably overlain by Kayrunnera Group.|Dark grey-green mafic outcrops of gabbro, dolerite; football-sized E-MORB pillow lavas with sparse and small vesicles; basaltic flows, basic tuffs, basaltic to doleritic sills.|
73421|Bittles Tank Volcanics|66918|5|Briefly described|Map legend|Cambrian||Three un-named units are mapped separately.||Unit in Ponto Group.||Map key shows: Overlies Baroorangee Creek Formation. Is overlain by Grasmere Formation.|Variably deformed mafic intrusives, and extrusive lavas with a tholeiitic geochemical affinity: small dykes and plutons of dolerite; gabbro; porphyritic metabasalt with pillow textures.|25-SEP-13
73421|Bittles Tank Volcanics|67105|5|Briefly described|p650, 653-654, 658-659, 661, 665-666|Cambrian|Cambrian|Wonnaminta Zone, Koonenberry Belt. Geochemistry discussed.||Ponto Group.|||Basalt dykes and lavas, both tholeiitic (mainly) and alkaline.|
73421|Bittles Tank Volcanics|67208|5|Briefly described|Map legend.|Cambrian|Cambrian|||Unit in Ponto Group.|||Undifferentiated: variably deformed mafic intrusives, and extrusive mafic lavas with a tholeiitic geochemical affinity.|
73421|Bittles Tank Volcanics|67322|4|Described|p11, p13|Stage 9|Paibian|Age determined using SHRIMP zircon analysis of one intrusive rock.|496.3 +/- 3.1 Ma (SHRIMP  zircon: Black, 2005).|Unit in Ponto Group||Intrudes the Teltawongee and Grey Range Groups.|Consists of enriched mid-ocean ridge basalts, tholeiitic pillow lavas, basaltic flows and basic tuffs. Also included in this unit are intrusive basaltic to doleritic sills.|21-FEB-18
73421|Bittles Tank Volcanics|69961|5|Briefly described|Map legend|Cambrian|Cambrian|No outcrop in map area. Three facies are mapped separately.||Unit in Ponto Group.|||Undifferentiated: variably deformed mafic intrusions, and extrusive mafic, tholeiitic lavas; coarse- and fine-grained gabbros and dolerites, and strongly magnetic phyllite.|
73421|Bittles Tank Volcanics|70648|5|Briefly described|Map Legend|Cambrian|Cambrian|3 un-named units: Coarse-grained, plagioclase with amphibole dominated gabbro to dolerite; relic pyroxene, amphibole and plagioclase; altered by epidote-carbonate-sericite or epidote-albite-chlorite-quartz; hornsfel contacts. Fine- to medium-grained, plagioclase with amphibole or pyroxene-dominated gabbro and dolerite; epidote-carbonate-sericite alteration, hornfels contacts. Pale to dark green-grey, variably cleaved, fine-grained porphyritic metabasalt, with plagioclase phenocrysts to >1cm; mm scale vesicles and pillow textures; weakly magnetic; widely distributed.||Ponto Group|Includes 3 un-named units.||Variably deformed mafic intrusions, and extrusive mafic lavas with a tholeiitic geochemical affinity.|
73421|Bittles Tank Volcanics|70650|5|Briefly described|Map Legend|Cambrian|Cambrian|3 unnamed subunits: Small dykes and plutons of diorite with clear intrusive relationship with country rocks (Ponto and Grey Range Group phyllite); restricted to south of Cymbric Vale homestead. Fine- to medium-grained, plagioclase with amphibole or pyroxene dominated gabbro and dolerite; epidote-carbonate-sericite alteration; hornfelsed contacts. Pale to dark green-grey, variably cleaved, fine-grained porphyritic metabasalt, with plagioclase phenocrysts to >1cm; mm scale vesicles and pillow textures; weakly magnetic; widely distributed throughout Ponto Group.||Ponto Group|Includes 3 un-named units.||Variably deformed mafic intrusives, and extrusive mafic lavas with a tholeiitic geochemical affinity.|
73421|Bittles Tank Volcanics|70651|5|Briefly described|Map Legend|Cambrian|Cambrian|5 unnamed sub-units: Fine- to medium-grained, plagioclase with amphibole or pyroxene-dominated intrusions with epidote-carbonate-sericite alteration, hornfels contacts. Green-grey cleaved metadolerite intrusions. Phyllite; epidote-pyrite-quartz alteration, epidote veins, calcite amygdules. Variably cleaved mafic rock in Willandra region. Porphyric metabasalt with plagioclase phenocrysts >1cm. ||Ponto Group|Includes 5 unnamed sub-units.||Variably deformed mafic intrusions, and extrusive mafic lavas with a tholeiitic geochemical affinity.|
73421|Bittles Tank Volcanics|70838|4|Described|p269-270|Cambrian|Cambrian|Koonenberry Belt.|c.510 Ma.|Ponto Group.||Is overlain unconformably by Kayrunnera Group.|Discontinuous lenses of tholeiitic to alkaline basalt.|
73421|Bittles Tank Volcanics|71262|6|Mentioned|p9 Fig 7|Cambrian|Cambrian|Map symbol suggests part of Ponto Group.||||||
73421|Bittles Tank Volcanics|73093|5|Briefly described|map legend|Cambrian|Cambrian||||||Dykes and plutons of foliated diorite; coarse-grained gabbro to dolerite; green-grey cleaved magnetic metadolerite; Green-grey, variably cleaved, fine-grained porphyritic metabasalt.|09-DEC-21
73421|Bittles Tank Volcanics|73177|6|Mentioned|1115 Fig.17|Cambrian|Cambrian|||Ponto Group.||||30-AUG-22
34791|Black Hill Gabbroic Complex|22945|6|Mentioned|p8|||Mentioned under - Area C geology.||||||
34791|Black Hill Gabbroic Complex|24509|5|Briefly described|p39 Fig. 1, p40, p42 Tab.1|Early Ordovician|Early Ordovician|Diorite. Age: 489+/-10Ma (isochron age). Geological Province: Murray Basin.||||||04-MAY-05
34791|Black Hill Gabbroic Complex|60567|5|Briefly described|p38|||||||||
24727|Black Hill Norite|22928|6|Mentioned|48|||||||||
24727|Black Hill Norite|23731|6|Mentioned|p51|||||||||
24727|Black Hill Norite|23869|5|Briefly described|p15 Fig. 3|Ordovician|Ordovician|||||||
24727|Black Hill Norite|24334|5|Briefly described|p48 Tb.1|Tremadoc|Tremadoc|Age: 495 - 501 Ma||||||
24727|Black Hill Norite|32457|4|Described|p103|||Rb/Sr age 487 +/- 5 Ma. K/Ar biotite age 486 Ma.||||||01-APR-14
24727|Black Hill Norite|42222|6|Mentioned|p26|||||||||
24727|Black Hill Norite|42246|6|Mentioned|p10|||||||||
24727|Black Hill Norite|42275|5|Briefly described|p466|||||||||
24727|Black Hill Norite|42884|5|Briefly described|Fig.1 P11|||||||||
24727|Black Hill Norite|43587|6|Mentioned|p166||Early Ordovician|||||||
24727|Black Hill Norite|44133|5|Briefly described|p51 Fig. 7.18, 56 Table 7.3|Ordovician|Ordovician|Mafic intrusive.  Coarse-grained gabbro, norite. Age: 486Ma, 476 +/- 5, 490 +/- 39Ma.||||||
24727|Black Hill Norite|50244|6|Mentioned|p100|Cambrian|Cambrian|Age: ~490Ma (Schmidt et al. 1993).||||||22-APR-09
24727|Black Hill Norite|64571|6|Mentioned|p840|Early Ordovician|Early Ordovician|Age: 490Ma.||||||15-DEC-08
24727|Black Hill Norite|67030|4|Described|p409, p412, p413,Tab. 2, p415|Tremadocian|Cambrian|Magnetic and age information presented for comparison (Schmidt et al. 1993). Related to a suite of bi-modal, dominantly A-type affinity, magmas from which the zircon age is derived. Thought to have intruded in the waning phases of the Delamerian Orogeny. Age shown as Cambrian in Fig 7.|485 Ma (radiometric, zircon)|||||12-DEC-21
24727|Black Hill Norite|67536|5|Briefly described|Map Legend|Darriwilian|Stage 3|Kanmantoo Province; basement to Murray Basin.|ca. 497 +/- 10 Ma - 482 +/- 20 Ma||||Late/post-Delamerian mafic-ultramafic intrusive rocks.|
24727|Black Hill Norite|70031|6|Mentioned|p246,250-251|||487+\-5 Ma date for late Cryogenian to post-Delamerian Orogeny poles. See p250 Table 2 for paleomagnetic analysis.||||||
24727|Black Hill Norite|70803|6|Mentioned|p3-p6|Ordovician|Cambrian|Occurs near the eastern margin of the "north-northwest trending G2 structural corridor gravity lineament."||||||
24727|Black Hill Norite|71322|5|Briefly described|p52 Fig.1|Ordovician|Cambrian|Late/post Delamerian.|497+/-10 Ma - 482+/-20 Ma.||||Mafic-ultramafic intrusive rocks.|
24727|Black Hill Norite|73093|5|Briefly described|map legend|Ordovician|Cambrian||||||Coarse-grained gabbro, norite.|09-DEC-21
24727|Black Hill Norite|73188|6|Mentioned|p310|||Bedrock outcrop on the uplifted Eba Block [Mount Lofty Ranges?].||||||
24185|Black Knob Marble|22926|6|Mentioned|42|||||||||
24185|Black Knob Marble|24175|3|Fully described|p8|Neoproterozoic|Neoproterozoic|Of Arkaroola Subgroup.  Max. thickness: 25m.||||||
24185|Black Knob Marble|24321|5|Briefly described|Map legend|Adelaidean|Adelaidean|Parent: Arkaroola Subgroup.||||||13-FEB-08
24185|Black Knob Marble|37854|2|Defined|p8|Adelaidean|Adelaidean|Early Willouran||||||
24185|Black Knob Marble|40294|6|Mentioned|Table 1|||||||||
24185|Black Knob Marble|41402|6|Mentioned|p42|||||||||
24185|Black Knob Marble|41403|5|Briefly described|p50|||||||||
24185|Black Knob Marble|42087|5|Briefly described|Fig.2 P15|||||||||
24185|Black Knob Marble|42222|5|Briefly described|p11|||||||||
24185|Black Knob Marble|42223|6|Mentioned|Fig.2 P36|||||||||
24185|Black Knob Marble|42238|5|Briefly described|Table 1 P75|||||||||
24185|Black Knob Marble|43052|5|Briefly described|p172, Table 6.1|||Of Arkaroola Subgroup.||||||13-FEB-08
24185|Black Knob Marble|43742|6|Mentioned|p42|||||||||
24185|Black Knob Marble|60718|6|Mentioned|p49, p53 Fig. 4|||Present as xenoclasts in the megbreccia of Breaden Hill.||Of Arkaroola Subgroup (Callanna Group) or correlated with it?||||15-APR-11
24185|Black Knob Marble|64796|5|Briefly described|p187, p188 fig 6, p194 Tb.2|Neoproterozoic|Neoproterozoic|Isolated marble blocks mapped by Murrell (1977) and defined by Forbes et al. (1981).||Of Arkaroola Subgroup.|||Isolated large blocks of calcitic marble.|
24185|Black Knob Marble|69019|5|Briefly described|p36.|Neoproterozoic|Neoproterozoic|Mapped by Murrell (1977) and Rowlands et al. (1980); defined by Forbes et al. (1981). Occurs as disrupted blocks within diapiric megabreccia.||Unit in Arkaroola Subgroup.|||Black to pale grey, fine- to medium-grained, calcitic marble or recrystallised dolomitic limestone; locally cupriferous.|
24185|Black Knob Marble|72456|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Marree 1:250k map sheet. |||||Marble, black, carbonaceous, calcitic. Smoky quartz, potash feldspar, in some beds. Chalcedonic nodules in some bedding planes.|
24185|Black Knob Marble|73222|6|Mentioned|p7|Tonian|Tonian|Adelaide Rift Complex, Willouran Ranges. Willouran.||Arkaroola Subgroup, Callanna Group, Warrina Supergroup||Unconformably overlain by Noranda Volcanics. Possibly equivalent to Wywyana Formation.||
75079|Black Maria Formation|62993|4|Described|p3, 6, 13-15, 18, 20. 37, 39, 40, 43|Paleoproterozoic|Paleoproterozoic|Olary Domain. Named after Black Maria Mine.|~1710 Ma (SHRIMP)|Raven Hill Subgroup|||Metasandstone, pelite-psammopelite with thin psammite layers locally exhibiting graded bedding; locally albititic.|19-DEC-21
75079|Black Maria Formation|64741|5|Briefly described|p301 Fig. 4, p309|Paleoproterozoic|Paleoproterozoic|Of Raven Hill Subgroup (Saltbush Group). Geological province: Olary Domain. Psammite-dominated unit.||||||07-FEB-11
75079|Black Maria Formation|64944|4|Described|p28 Fig. 1, p29 Tb. 1|Paleoproterozoic|Paleoproterozoic|Of Raven Hill Subgroup (Saltbush Group). Geological province: Olary Domain. Psammite, psammopelite and pelite, locally graphitic and locally with calcsilicate ellipsoids.||||||07-FEB-11
75079|Black Maria Formation|66302|6|Mentioned|p36 Fig.9, p39|Statherian|Statherian|Olary Domain, Curnamona Province. ||Raven Hill Subgroup||||
75079|Black Maria Formation|70405|4|Described|p9 table 1, p28, p29,p31 plate 9, p41,|Paleoproterozoic|Paleoproterozoic|||Raven Hill Subgroup||Underlies Oonartra Creek Formation|Pelite interbedded with fine- rarely medium grained feldspathic (albitic) psammite; finely graphitic pelitic schist. Psammite beds are occasionally graded.|
75079|Black Maria Formation|70657|4|Described|p14-15, p21, p33-34, p40-41, p44|Statherian|Statherian|New name. Curnamona Province, Olary Domain. Is separated from over- and under-lying Formations by graphitic units.|<1693+/-3 Ma - >1655 Ma|Raven Hill Subgroup||Overlies Plumbago Formation (Larry Macs Subgroup). Underlies Oonartra Creek Formation. With Oonartra Creek Formation is equivalent to Purnamoota Subgroup (Broken Hill Domain).|Dominantly psammitic and locally albitic; variable pelitic interbeds. Laterally lithologically variable including dark grey psammite; units locally crowded with calcsilicate and baritic ellipsoids.|
75079|Black Maria Formation|70658|5|Briefly described|p3, 7, 15|Paleoproterozoic|Paleoproterozoic|Olary Domain, Curnamona Province.||Raven Hill Subgroup.||Locally overlies Plumbago Formation.||
29821|Blackfellow Hill Pyroxenite|24472|5|Briefly described|p5 Tb.1|Archean|Archean|Geological Province: Harris Greenstone Domain, Gawler Craton. Age: 2453 Ma. Parent: Mulgathing Complex.||||||07-NOV-08
29821|Blackfellow Hill Pyroxenite|43052|4|Described|p43, Table 3.2|||Of Mulgathing Complex||||||
29821|Blackfellow Hill Pyroxenite|50605|5|Briefly described|p8.7|||Of the Mulgathing Complex. Geological Province: Gawler Craton & Curnamona Province.||||||01-MAR-10
29821|Blackfellow Hill Pyroxenite|65376|5|Briefly described|p190, pp198-202.||||2461 +/- 5 Ma; metamorphosed c.2435-2425 Ma.|Unit in Mulgathing Complex.|||Garnet-bearing mafic gneiss, metagabbro, metapyroxenite, metanorite.|
29821|Blackfellow Hill Pyroxenite|65385|6|Mentioned|pS132|Siderian|Siderian|Of Mulgathing Complex. Synorogenic magmatism. ~2460 Ma.||||||08-FEB-17
29821|Blackfellow Hill Pyroxenite|66302|6|Mentioned|p12|Siderian|Siderian||2461 +/- 5 Ma (SHRIMP U-Pb, Kositicin 2010)|||||
29821|Blackfellow Hill Pyroxenite|66526|5|Briefly described|p37.|Proterozoic|Proterozoic|Central Gawler Province, with correlative in the Weeli Wolli Formation of Pilbara Province. Produced in the Weeli Wolli Event, ME 1 in the Proterozoic Mafic-Ultramafic Magmatic Event Series.|c.2455 Ma.|||||
29821|Blackfellow Hill Pyroxenite|67980|5|Briefly described|p561 Tb.3|Siderian|Siderian|Christie Domain, Gawler Craton. Igneous crystallisation age by Fanning et al. (2007).|2461 +/- 5 Ma (U-Pb SHRIMP zircon).|||||08-FEB-17
29821|Blackfellow Hill Pyroxenite|68128|6|Mentioned|p2, p20, p84|Palaeoproterozoic|Archaean|Gawler Craton. Ultramafic intrusions into this unit bore traces of Ni-Cu sulphide mineralisation.||Mulgathing Complex||||
29821|Blackfellow Hill Pyroxenite|73230|5|Briefly described|p10, p16|||Superseded by Skuse Hill Metapyroxenite. Unit name considered culturally exclusive and socially inappropriate. [Also written as 'Blackfellow Hill Pyroxenite'].||||||
39563|Blowhole Creek Member|24465|4|Described|p348|Early Cambrian|Early Cambrian|Of Carrickalinga Head Formation Replaces Blowhole Creek Siltstone Member. Conformably overlies Magidan Inlet Member. Includes the Milendella Member.|||||Mainly siltstone with minor thin to lenticular fine sandstone beds.|06-NOV-15
39563|Blowhole Creek Member|63848|6|Mentioned|p534 Fig.4.|||||Unit in Carrickalinga Head Formation.||Overlies Madigan Inlet Member.||
83510|Blue Duck Group|73155|5|Briefly described|p265, p274-275, p282 Fig.13, p283-286|Statherian|Statherian|Mount Woods Domain, southern. Not a formalised stratigraphic name. May be part of same stratigraphic package as Skylark Metasediments and Kennedy's Dam Group with broad equivalence between them. Generally low magnetic response, smooth texture, rare magnetic marker horizons; occurs in a narrow linear belt. Extensively brecciated and altered around Prominent Hill IOCG deposit. Interpreted as part of hangingwall/upper plate of Mount Woods Metamorphic Core Complex. Location in text includes p277-278.|ca. 1750 Ma maximum depositional age|||Faulted against Gawler Range Volcanics.|Calc-silicate, iron formation and feldspathic metasediments. Includes Fe-pelites, calc-silicates and siliciclastics.|
25795|Blue Mine Conglomerate|22772|5|Briefly described|Table13.1|Cryogenian|Cryogenian|||||||
25795|Blue Mine Conglomerate|22857|5|Briefly described|Tb. 13.1 (insert p70-71)|Torrensian|Torrensian|Of the Emeroo Subgroup (Burra Group).||||||
25795|Blue Mine Conglomerate|22869|6|Mentioned|P46|||Correlated to the Carey Gully Sandstone Member||||||
25795|Blue Mine Conglomerate|22889|6|Mentioned|p31|Adelaidean|Adelaidean|Parent - Emeroo Subgroup.  Blue Mine Conglomerate of the northern Flinders Ranges.||||||
25795|Blue Mine Conglomerate|23394|5|Briefly described|Map legend|Proterozoic|Proterozoic|||||||
25795|Blue Mine Conglomerate|23411|6|Mentioned|Map Legend|||||||||
25795|Blue Mine Conglomerate|23818|5|Briefly described|p55|||Max. thickness: 1300 ft. Overlying unit: Opaminda Siltstone.||||||
25795|Blue Mine Conglomerate|24176|4|Described|p10, p25 Tb. 1|Adelaidean|Adelaidean|Of Callana Beds.  Arkosic conglomerate, minor quartzites and grey siltstones.  Overlies Woodnamoka Phyllite.  Age is Willouran.  Max. thickness: 460m.  Geological Province: Mount Painter Province.||||||
25795|Blue Mine Conglomerate|24546|5|Briefly described|p2 - 3 Fig.2|Neoproterozoic|Neoproterozoic|Arkositic conglomerate. Of Burra Group. Overlies Woodnamoka Phyllite and Humanity Seat Formation. Geological Province: Adelaide Fold Belt.||||||16-JAN-08
25795|Blue Mine Conglomerate|24593|5|Briefly described|p613 Fig. 1b|Adelaidean|Adelaidean|Of the Burra Group.  Geological Province: Mount Painter Inlier.||||||
25795|Blue Mine Conglomerate|30176|6|Mentioned|Map legend|Adelaidean|Adelaidean|Willouran||||||
25795|Blue Mine Conglomerate|30177|2|Defined|p128|Adelaidean|Adelaidean|See also p62. Type section: Approximately half a mile northeast of Arkaroola Homestead, north side of Kingsmill Creek, lat. 30degrees 19'19"S long. 139degrees 22'16"E to lat. 30degrees19'32"S long.139degrees 22'01E [assumed AGD 66]||||||25-NOV-22
25795|Blue Mine Conglomerate|30801|6|Mentioned|p5|||Upper Callanna Beds. Table P5-6||||||
25795|Blue Mine Conglomerate|30807|6|Mentioned|p103|||Suggested map symbol.||||||
25795|Blue Mine Conglomerate|32724|6|Mentioned|Fig.1|||Willouran. Correlation||||||
25795|Blue Mine Conglomerate|32823|6|Mentioned|p362|||||||||
25795|Blue Mine Conglomerate|33474|6|Mentioned|Fig.4|||||||||
25795|Blue Mine Conglomerate|34535|5|Briefly described|p55|||||||||
25795|Blue Mine Conglomerate|35255|6|Mentioned|p13|||See also Fig.7.||||||
25795|Blue Mine Conglomerate|36733|6|Mentioned|Table 5|||||||||
25795|Blue Mine Conglomerate|37854|6|Mentioned|Table 1|||||||||
25795|Blue Mine Conglomerate|38157|6|Mentioned|Table III|||||||||
25795|Blue Mine Conglomerate|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Torrensian||||||
25795|Blue Mine Conglomerate|39352|6|Mentioned|Map legend|Adelaidean|Adelaidean|Torrensian||||||
25795|Blue Mine Conglomerate|40294|6|Mentioned|p9|||||||||
25795|Blue Mine Conglomerate|41403|6|Mentioned|p43|||||||||
25795|Blue Mine Conglomerate|41404|3|Fully described|p86|||||||||
25795|Blue Mine Conglomerate|41405|5|Briefly described|p133|||||||||
25795|Blue Mine Conglomerate|42222|5|Briefly described|p13|||||||||
25795|Blue Mine Conglomerate|43052|5|Briefly described|p177,Table 6.1|||of Emeroo Subgroup||||||
25795|Blue Mine Conglomerate|61523|5|Briefly described|p12|Adelaidean|Adelaidean|Geological Province: Mount Painter Province.||||||
25795|Blue Mine Conglomerate|65925|5|Briefly described|p124 Fig.3, p125, Appendix 2.|||||Unit in Burra Group.||Is overlain by Opaminda Formation.|Conglomerate, pink, heavy-mineral laminated, arkosic; minor sandstone; dark grey laminated siltstone.|
25795|Blue Mine Conglomerate|70384|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Adelaide Geosyncline. Age shown more specifically as Torrensian [Cryogenian].||Emeroo Subgroup.||Conformably? overlies Woodnamoka Phyllite. Is overlain conformably? by Opaminda Formation.|Conglomerate, pink, heavy mineral laminated, arkosic; minor sandstone; dark grey laminated siltstone.|18-JAN-19
25795|Blue Mine Conglomerate|74367|5|Briefly described|p7 Fig.6, p8-9, p12-14, p16, p20|Tonian|Tonian|LA-ICP-MS detrital zircon MDA of 1106+/-85 Ma is much older than the true depositional age.||Emeroo Subgroup||||
24737|Blue Range beds|41363|6|Mentioned|p16|||||||||
24737|Blue Range beds|41667|5|Briefly described|p6|||||||||
24737|Blue Range beds|42738|5|Briefly described|map legend|Mesoproterozoic|Mesoproterozoic|Fluvial. Basal conglomerate contains well-rounded clasts of quartz, quartzite and chert in an arkosic and micaceous matrix. Extensively mottled mauve and white.||||Probably equivalent to Corunna Conglomerate.|Massive to cross-bedded white sandstone and gritty conglomeratic sandstone with abundant angular feldspar detritus. Rare veins of hematite.|30-JUL-21
24737|Blue Range beds|43053|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Sandstone, conglomerate.||||||26-MAY-05
24737|Blue Range beds|43258|5|Briefly described|Map Legend||Mesoproterozoic|||||||
24737|Blue Range beds|43298|5|Briefly described|Map Legend||Mesoproterozoic|||||||
24737|Blue Range beds|60953|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Sandstone, conglomerate (age uncertain).||||||07-NOV-08
24737|Blue Range beds|61070|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Fluvial gritty sandstone and conglomerate, minor siltstone. Deposited in Itiledoo Basin. Possibly equivalent to Corunna Conglomerate, Pandurra Formation. Geological Province: Gawler Craton.||||||12-JAN-10
24737|Blue Range beds|61108|5|Briefly described|map legend|||Sandstone, conglomerate. Age uncertain.||||||
24737|Blue Range beds|61556|5|Briefly described|p9-10 Figure|||||||||
24737|Blue Range beds|63020|5|Briefly described|p987 Fig. 8|Mesoproterozoic|Mesoproterozoic|Age: <1600Ma. Geological Province: Gawler Craton (Nuyts Domain and Cleve Domain).||||||10-AUG-07
24737|Blue Range beds|65220|6|Mentioned|p22 Fig.4|Mesoproterozoic|Paleoproterozoic|In the Eyre Peninsula region. Age poorly constrained, but may conceivably be of similar age to the Corunna Conglomerate||||||10-DEC-09
24737|Blue Range beds|65376|6|Mentioned|p17. |Mesoproterozoic|Mesoproterozoic|||||||
24737|Blue Range beds|66302|5|Briefly described|p33, p34, p43, p46|Calymmian|Statherian|Cleve and Coulta Domains, Gawler Craton. |1605 +/- 9 Ma (SHRIMP, Fraser and Neumann, 2010)||||Sandstone.|
24737|Blue Range beds|67181|5|Briefly described|p616 Fig.1|Mesoproterozoic|Mesoproterozoic|Gawler Craton. References: Fairclough et al. 2003, Payne et al. 2003.||||||
24737|Blue Range beds|69048|6|Mentioned|p2|Mesoproterozoic|Mesoproterozoic|Southern Eyre Peninsula.||||||
24737|Blue Range beds|73027|6|Mentioned|p12 fig 1.5,|Mesoproterozoic|Mesoproterozoic|Gawler Craton.||||||
24737|Blue Range beds|73103|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic||||||Sandstone, minor grit and pebble beds, white, massive to cross-bedded, rare haematite veins.|
38064|Blue Whale Supersequence|24336|5|Briefly described|p99 Fig.3|||Correlated to the Ceduna Formation.||||||
38064|Blue Whale Supersequence|61544|6|Mentioned|p367 Fig.3. |Albian|Albian|Ceduna Sub-basin. Accelerated subsidence.||||Overlies Bronze Whaler Supersequence. Is overlain by White Pointer Supersequence.||
38064|Blue Whale Supersequence|66578|6|Mentioned|p1007 Fig.3.|Cretaceous|Cretaceous|Ceduna Sub-Basin, Bight Basin.||||Overlies Bronze Whaler Supersequence. Is overlain by White Pointer Supersequence.||
38064|Blue Whale Supersequence|69297|5|Briefly described|p14 fig 2.4, p23, p25 fig 2.9|Cenomanian|Albian|Eyre, Ceduna and Duntroon Sub-basins. Deposited in marine to deltaic environments during the first marine flooding event of the Ceduna Sub-basin. Good potential oil and gas source rocks with high organic content. Interpreted pre-deformation thickness of 1500-2000m. See also p26 fig 2.11, p41, p43, p44, p45 fig 2.17, p58, p60, p61.||||Overlies the Bronze Whaler Supersequence. Overlain by the White Pointer Supersequence.||
38064|Blue Whale Supersequence|70067|5|Briefly described|Ceduna: Fig.2; p2. Regional: Fig.2; p2|Cenomanian|Albian|Bight Basin. Comprises Ceduna Formation and topmost Upper Borda Formation. Marine shales are potential source rocks and form a regional seal.||||Overlies Bronze Whaler Supersequence. Is overlain by White Pointer Supersequence.|Marine silts and shales were widely deposited.|
38064|Blue Whale Supersequence|71618|6|Mentioned|p131|Cenomanian|Albian|Of Bight Basin, Madura Shelf..||||||05-SEP-19
34747|Boconnoc Siltstone Member|22889|4|Described|p38|Adelaidean|Adelaidean|See p38-39 for location of type section and details of new stratigraphic unit. The Boconnoc Siltstone Member superseds the former Boconnoc Formation as the unit has been down graded from formation to member status, see p 33 for details of change.||||||
26411|Bolla Bollana Tillite|22510|5|Briefly described|table1, p38|||Age: Sturtian. Northern Flinders Ranges.||||||
26411|Bolla Bollana Tillite|23804|6|Mentioned|p17|||||||||
26411|Bolla Bollana Tillite|24175|3|Fully described|p12|Neoproterozoic|Neoproterozoic|Massive diamictite of the Yudnamutana Subgroup.  Overlain by Wilyerpa Formation; unconformably underlies the Burra Group.  Max. thickness: 204m.||||||05-JUL-13
26411|Bolla Bollana Tillite|24321|5|Briefly described|Map legend|Proterozoic|Proterozoic|Parent: Yudnamutana Subgroup||||||
26411|Bolla Bollana Tillite|30178|6|Mentioned|p19|||||||||
26411|Bolla Bollana Tillite|35255|6|Mentioned|p13|||||||||
26411|Bolla Bollana Tillite|36733|6|Mentioned|Table 5|||||||||
26411|Bolla Bollana Tillite|37932|5|Briefly described|p539|||||||||
26411|Bolla Bollana Tillite|38157|6|Mentioned|Table IV|||||||||
26411|Bolla Bollana Tillite|39344|6|Mentioned|Map legend|Precambrian|Precambrian|Sturtian||||||
26411|Bolla Bollana Tillite|40294|6|Mentioned|p41|||||||||
26411|Bolla Bollana Tillite|41405|3|Fully described|p132|||||||||
26411|Bolla Bollana Tillite|41526|6|Mentioned|p43|||||||||
26411|Bolla Bollana Tillite|41647|6|Mentioned|p834|||||||||
26411|Bolla Bollana Tillite|42222|5|Briefly described|p16|||||||||
26411|Bolla Bollana Tillite|42238|5|Briefly described|p73|||||||||
26411|Bolla Bollana Tillite|42813|6|Mentioned|p17|||||||||
26411|Bolla Bollana Tillite|43052|5|Briefly described|p183,Table 6.1|||of Yudnamutana Subgroup||||||
26411|Bolla Bollana Tillite|62903|6|Mentioned|p729|Sturtian|Sturtian|Adelaide Rift Complex. Sturtian glaciation (Preiss et al. 1998) correlates with Areyonga Formation. Presented in text as Sturt-Appila-Pualco-Bolla Bollana-Merirjina Tillites.||Yudnamutana Subgroup||Sturtian glacial units overlain by Tapley Hill Formation||
26411|Bolla Bollana Tillite|67180|6|Mentioned|p602 Fig.2|Cryogenian|Cryogenian|Sturtian age, of Northern Flinders Ranges (Preiss et al. 1998).||Unit in Umberatana Group||||
26411|Bolla Bollana Tillite|68068|5|Briefly described|Map legend|Sturtian|Sturtian|Adelaide Geosyncline.||Unit in Yudnamutana Subgroup.||Overlies Fitton Formation gradationally. Is unconformably overlain by Balcanoona Formation.|Massive tillite, lithic and quartz clasts with slaty to sandy matrix; clasts subangular to well-rounded, partly deformed by folding; minor tillitic siltstone and quartzite are metamorphosed to calc-silicate and para-amphibolite lenses and beds.|
26411|Bolla Bollana Tillite|69019|3|Fully described|p41-45, p134.|Neoproterozoic|Neoproterozoic|Of Coats and Forbes (1977); formerly Bolla Bollana Formation (Coats 1964). Outcrops around Mt. Babbage; type section is NW from Valley Bore. Sediments sourced from Curnamona Province to the E and SE; possibly also the Muloorina Ridge to the N. Local sulfide mineralisation in cherty pods and beds.||Unit in Yudnamutana Subgroup.||Conformably overlies Fitton Formation. Is overlain conformably by Wilyerpa Formation, and unconformably by Yankaninna or Balcanoona Formations.|Massive boulder-bearing greywacke with clay-rich matrix, boulders angular to rounded, matrix supported; above is smaller boulders confined to broad bands and numerous meta-sandstone interbeds; top is mainly dark grey greywacke with clay-rich matrix.|
26411|Bolla Bollana Tillite|69023|3|Fully described|p64-66,p68-69,p77,p86-88,p137,p146,p154|Neoproterozoic|Neoproterozoic|Of Coats and Forbes (1977); originally Bolla Bollana Formation (Coats, 1964). Type section is NW from Valley Bore. Thickness ~1500m. Mid- to late-Sturtian age is assigned on stratigraphic grounds; no radiometric age. Generally forms rounded, moderately sized hills, with a quartzite boulder surface lag. Supplied by sulphide-bearing hot brine sea-floor emanations.||Unit in Yudnamutana Subgroup.||Gradationally overlies Fitton Formation. Is overlain by Balcanoona or Yankaninna Formations (unconformably or disconformably).|Tillite. Basal massive boulder-bearing greywacke; matrix-supported. Boulders are angular to rounded; matrix is dark grey to dark bluish-grey shale, lesser silt and/or sand. Also a series of amphibolitic to calc-silicate tillite beds or lenses.|
26411|Bolla Bollana Tillite|70384|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Adelaide Geosyncline. Close to the basal contact is a feldspathic quartzite bed, medium- to coarse-grained; this, and the other two facies, are mapped separately. Age shown more specifically as Sturtian [Cryogenian].||Yudnamutana Subgroup.||Gradationally overlies Fitton Formation.|Massive diamictite, clasts (usually tectonically flattened) mostly quartz +/- lithics, dark grey shale-slate matrix, +/- grey to yellow sandstone interbeds. Minor siltstone and quartzite interbeds, some altered to calc-silicate or para-amphibolite.|21-JAN-19
26411|Bolla Bollana Tillite|72456|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Marree 1:250k map sheet. |||||Tillite, massive boulder tillite, with high boulder content, gritty sub-greywacke matrix, minor quartzite and laminated siltstone.|
26411|Bolla Bollana Tillite|73234|6|Mentioned|p20|||||||Overlain by Wilyerpa Formation.|Tillitic.|
26411|Bolla Bollana Tillite|74367|5|Briefly described|p7-9, p11, p14-16, p20-21|Cryogenian|Cryogenian|Misspelt Bolla Bollana Formation p7.|673+/-19 Ma LA-ICP-MS detrital zircon MDA|Yudnamurtana Subgroup||||
39570|Bollaparudda Subgroup|24465|2|Defined|p360, p363 App.1|Early Cambrian|Early Cambrian|Upper subgroup of the Kanmantoo Group.  Includes Talisker, Tapanappa, Tunkalilla, Balquhidder, Petrel Cove and Middleton Formations.||||||27-OCT-04
39570|Bollaparudda Subgroup|65664|5|Briefly described|p1096, p1104-5, p1106 Fig.5|Early Cambrian|Early Cambrian|Possibly a structural repetition of Backstairs Passage Formation.||Of Kanmantoo Group.|Includes Talisker, Tapanappa, Tunkalilla, Balquhidder and Petrel Cove Formations, and Middleton Sandstone.|Unconformably overlies Keynes Subgroup.||09-MAY-12
39570|Bollaparudda Subgroup|70865|6|Mentioned|p2|||Adelaide Hills area. Mis-spelled as Boolaparudda Subgroup.||||||
39570|Bollaparudda Subgroup|73188|5|Briefly described|p316, p343|Early Cambrian|Early Cambrian|Mount Lofty Ranges.||Kanmantoo Group|Middleton Sandstone, Petrel Cove Formation, Balquihidder Formation, Tunkalilla Formation, Tapanappa Formation, Talisker Formation|||
67915|Boongar beds|44133|5|Briefly described|p40|||Equivalent to/correlated with: Mount Chandler Sandstone. ||||||
27311|Boorloo Siltstone|22772|5|Briefly described|Table13.1|Cryogenian|Cryogenian|||||||
27311|Boorloo Siltstone|22857|5|Briefly described|Tb. 13.1 (insert p70-71)|Willouran|Willouran|Of the Curdimurka Subgroup (Callanna Group).||||||
27311|Boorloo Siltstone|24175|3|Fully described|p10|Neoproterozoic|Neoproterozoic|Of Curdimurka Subgroup. Overlies Cooranna Formation.  Max. thickness: 519m.||||||13-FEB-08
27311|Boorloo Siltstone|24321|5|Briefly described|Map legend|Adelaidean|Adelaidean|Parent: Curdimurka Subgroup.||||||13-FEB-08
27311|Boorloo Siltstone|37854|2|Defined|p12|Adelaidean|Adelaidean|See P9.Prob.Late Willouran||||||
27311|Boorloo Siltstone|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Willouran||||||
27311|Boorloo Siltstone|40294|6|Mentioned|p9|||See also Table 1||||||
27311|Boorloo Siltstone|41402|6|Mentioned|p42|||||||||
27311|Boorloo Siltstone|41403|4|Described|p65|||||||||
27311|Boorloo Siltstone|42087|5|Briefly described|p13|||See also Fig.2||||||
27311|Boorloo Siltstone|42222|5|Briefly described|p12|||||||||
27311|Boorloo Siltstone|42238|5|Briefly described|p72|||||||||
27311|Boorloo Siltstone|43052|5|Briefly described|p175,Table 6.1|||Of Curdimurka Subgroup.||||||13-FEB-08
27311|Boorloo Siltstone|60718|5|Briefly described|p49 Fig. 2, p50, 52, 53|Adelaidean|Adelaidean|Geological Province: Adelaide Geosyncline.||Of Curdimurka Subgroup (Callanna Group).||||15-APR-11
27311|Boorloo Siltstone|64796|6|Mentioned|p190 Fig.8, p194 Tb.2, p200 Fig.10, p202|Neoproterozoic|Neoproterozoic|Willouran Ranges. Appears in Fig.8 without the lithology.||Unit in Curdimurka Subgroup.||Overlies Cooranna Formation.||
27311|Boorloo Siltstone|64797|6|Mentioned|p161 Tb.4|||Adelaide Rift Complex. Lithology/rank not shown on diagram. S-isotope data. ||||||
27311|Boorloo Siltstone|69019|4|Described|p37-38.|Neoproterozoic|Neoproterozoic|Forbes (1980). 519 m thick. Type section W of Boorloo coppper workings.||Unit in Curdimurka Subgroup.||Is faulted against or unconformably underlies Burra Group.|Dark grey to black laminated siltstone, carbonaceous with thin planar dolomite bands; marker bed of fine-grained sandstone-quartzite; near-basal micrite member of limestone, dolomite and siltstone.|
27311|Boorloo Siltstone|72456|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Marree 1:250k map sheet. |||||Siltstone, laminated, carbonaceous, dark grey, thin planar dolomite bands.|
27311|Boorloo Siltstone|72492|3|Fully described|p2 Fig.1, p3, p3 Fig.2, p4 Fig.3a|Neoproterozoic|Neoproterozoic|In the Willouran Ranges. Tyoe section is located at 29.7264 S/137.9772E to 29.7238S/137.9821E, locally known as Gum Creek. Three additional sections are detailed on p3 and were dcorrelated by prominent carbonate ridges at the top of the unit as marker beds. This unit is stratigraphically variable and can be broadly subdivided into seven intervals at the type locality; summarised on p3. Compared with Kirwan Siltstone. See also p4 Fig.3c and f, p5 Fig.4g and h, p6, p7 Tb.1, p7 Tb.1, p9, p10 Tb.2, p11 Tb.3, p12-14 Tb.4,  p15 Fig.8, p16-17.||Curdimurka Subgroup||Overlies Cooranna Formation.|Includes black shale, stromatolites with desiccation cracks and ripples and interlaminated siltstone and shale with minor sandstone interbeds.|16-SEP-20
27311|Boorloo Siltstone|73222|6|Mentioned|p7|Tonian|Tonian|Willouran Ranges. Torrensian.||Curdimurka Subgroup, Callanna Group, Warrina Supergroup||Underlain by Cooranna Formation. Possibly equivalent to Waraco Limestone and Kirwan Siltstone.||
27311|Boorloo Siltstone|74367|6|Mentioned|p7 Fig.6|||||Curdimurka Subgroup||||
77136|Bopeechee Regolith|68068|5|Briefly described|Map legend|Early Jurassic|Late Permian|A widespread regolith of chemically altered rocks overlain by a mechanically derived debris. Exposed at edge of Flinders Ranges.||||Is overlain by Parabarana Sandstone.|White, cream, yellow to brown saprolite is strongly kaolinised; original rock fabric preserved by resistant minerals; discontinuous due to erosion; colluvium slope debris of angular fragments, unsorted, composition reflects underlying saprolite.|
77136|Bopeechee Regolith|69023|5|Briefly described|p85-88, p98, p101, p107|Mesozoic|Paleozoic|Defined by Krieg et al. (1991). Intensely chemically altered rock or sediment, commonly overlain by a mechanically derived colluvium. It is developed within Mesoproterozoic granites (eg Terrapinna Granite) and Neoproterozoic Adelaide Geosyncline metasediments (eg Bolla Bollana Tillite). Latest Permian to latest Jurassic age inferred.||||Is overlain by Parabarana Sandstone.|A lower bleached or pallid saprolite zone, white, cream, yellow to brown, is strongly kaolinised; commonly overlain by a colluvial slope debris unit, mainly yellow to brown; has Liesegang banding and ferruginous pisolith bands.|
77136|Bopeechee Regolith|70384|5|Briefly described|Map legend.|||Occurs at Flinders Ranges edges, within Proterozoic or Late Paleozoic rocks. Best exposures SW of Prospect Hill (S of Dog Fence), underlying the Parabarana Sandstone. Age: ?Late Permian to ?Early Jurassic from stratigraphic evidence.|||||Widespread weathered zone (in situ pedolith + saprolith), locally includes 0.1-1.5m thick colluvial top (+/- paleosol/slope debris), residual unsorted angular fragments +/- pseudo-layering; pallid saprolith strongly kaolinised.|
77136|Bopeechee Regolith|72456|5|Briefly described|Map Legend|Jurassic|Permian|Marree 1:250k map sheet.  Developed in mesoproterozoic granite or adelaidian metasediments.|||||Saprolite overlain by waste material or slope debris/colluvium.|
24194|Bosanquet Formation|22629|6|Mentioned|p149,150|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
24194|Bosanquet Formation|22690|6|Mentioned|P311||Orosirian|Age of unit is 1845+/-9 Ma||||||
24194|Bosanquet Formation|23285|5|Briefly described|p 333|||||||||
24194|Bosanquet Formation|23719|5|Briefly described|p15 Table 2|Orosirian|Orosirian|Age: 1845+/-9 Ma (U-Pb zircon). Geological Province: Gawler Craton.||||||
24194|Bosanquet Formation|41325|2|Defined|p12|Proterozoic||||||||
24194|Bosanquet Formation|41327|6|Mentioned|Fig.2|||||||||
24194|Bosanquet Formation|42738|5|Briefly described|map legend|Paleoproterozoic||||||||07-NOV-08
24194|Bosanquet Formation|43052|5|Briefly described|p61|||Of Hutchison Group? Age of 1845+/-9 Ma.||||||24-JUN-09
24194|Bosanquet Formation|43053|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Hutchinson Group. Rhyodacite. Geological Province: Gawler Craton.||||||07-NOV-08
24194|Bosanquet Formation|43258|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
24194|Bosanquet Formation|43298|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
24194|Bosanquet Formation|50605|5|Briefly described|p3.3|||Of the Hutchison Group. Geological Province: Gawler Craton & Curnamona Province.||||||
24194|Bosanquet Formation|60953|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Hutchison Group. Age: 1859Ma. Rhyodacite, calcsilicate.||||||07-NOV-08
24194|Bosanquet Formation|61108|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|Rhyodacite and calcsilicate rock. Age: 1859 Ma.||||||07-NOV-08
24194|Bosanquet Formation|62893|4|Described|Map Legend, p5, p10-13, p28-29|Early Proterozoic|Early Proterozoic|Probably belongs to the Hutchison Group based on age and some lithological similarity. Type section is in Broad View 1 drillhole (Rankin and Flint, 1987). Recognised in a 1 by 5 km zone east of Carappee Hill and is not known elsewhere. Has a U-Pb zircon age of 1845 +/- 9 Ma. Represents a period of contemporaneous acid volcanism and carbonate sedimentation with considerable conglomerate input. Dissimilar whole-rock geochemistry to other Palaeoproterozoic volcanics of the Gawler Craton. May be synchronous with deposition of the Upper Middleback Jaspilite. A megacrystic rhyodacite may represent the basal horizon.|||||Well banded, grey to green, calc-silicate gneiss interlayered with metavolcanics including grey, porphyritic rhyodacite and breccia containing clasts of rhyolite-rhyodacite, dolomite, calc-silicate, granite and chert in diopside-rich matrix.|
24194|Bosanquet Formation|63223|5|Briefly described|p16|Paleoproterozoic|Paleoproterozoic|Age: 1866+/-10Ma. Geological Province: Gawler Craton.||||||07-NOV-08
24194|Bosanquet Formation|63866|4|Described|p5, p9, p30|Orosirian|Orosirian|Cleve Domain. U-Pb age derived from Fanning et al., 2007. The contact with the rest of the Hutchison Group is not exposed.|1866 +/- 10 Ma (U-Pb zircon)|Hutchison Group||||
24194|Bosanquet Formation|64130|5|Briefly described|p1379|Orosirian|Orosirian||1866 +/- 10 Ma (Fanning et al., 2007).|Unit in Hutchison Group.|||Pelitic rocks and felsic volcanics.|
24194|Bosanquet Formation|64313|5|Briefly described|p450|Paleoproterozoic|Paleoproterozoic|Of the Hutchison Group. Intercalated volcanogenic unit. Age: 1866+/-10Ma (U-Pb crystallisation). Geological province: Gawler Craton. See also Fig. 1.||||||09-FEB-10
24194|Bosanquet Formation|65221|5|Briefly described|p26|Palaeoproterozoic|Palaeoproterozoic|within the uppermost Hutchison Group. Age 1866+/-10Ma||||||
24194|Bosanquet Formation|65375|5|Briefly described|p44.|||Felsic volcanics.|c.1852 Ma.|Unit in Hutchison Group.||||
24194|Bosanquet Formation|65376|5|Briefly described|p38, pp62- 64.|Paleoproterozoic|Paleoproterozoic||1866 +/- 10 Ma.|Uppermost unit in Hutchison Group.|||A sequence of interlayered, deformed and recrystallised rhyodacites and calcsilicate gneisses.|
24194|Bosanquet Formation|65390|6|Mentioned|p23 Fig.3|Orosirian|Orosirian|Cleve Domain, Gawler Craton. Age of 1860 Ma given.||||||
24194|Bosanquet Formation|66302|6|Mentioned|p24, p25, p26, p33|Orosirian|Orosirian|Cleve Domain, Gawler Craton. |1866 +/- 10 Ma (Fanning et al, 2007, SHRIMP U-Pb)|Hutchison Group||||
24194|Bosanquet Formation|66882|5|Briefly described|p101; p103 Fig.3a,c; p109-114|Orosirian|Orosirian|Isotope data. Geochemistry discussed. A-type; intracontinental magmatism.|Eruption age 1866+/-10 Ma (Fanning et al., 2007).|Darke Peak Group.||Overlies Yabmana Iron Formation. Is overlain disconformably by Cleve Group.|Succession of calcsilicate gneiss and porphyritic rhyolitic volcanic rocks.|
24194|Bosanquet Formation|67323|5|Briefly described|Eastern Australia Time-Space Plot; p30|||Gawler Craton. Eruption and deposition age.|1866 +/- 10 Ma.|Hutchison Group.|||Rhyolites and calc-silicates.|
24194|Bosanquet Formation|67721|5|Briefly described|p34|Orosirian|Orosirian||c. 1850 Ma||||Banded iron formations, shaly banded iron formations.|
24194|Bosanquet Formation|69048|6|Mentioned|p3|||Central-western Eyre Peninsula.|c.1865 Ma.|||||
24194|Bosanquet Formation|71037|6|Mentioned|p21 Fig.1|Paleoproterozoic|Paleoproterozoic|Shown only on 'Outcropping geology and mineral deposits of northern Eyre Peninsula' map p21 Fig.1.||||Shown as younger than Donington Suite and older than Hutchison Group.||
24194|Bosanquet Formation|71129|6|Mentioned|p18,23|Orosirian|Orosirian|Geological Province: Cleve-Coulta Domain, Gawler Craton. |1850 Ma|||Contemporaneous with Donington Suite.||
24194|Bosanquet Formation|71317|5|Briefly described|p16|Palaeoproterozoic|Palaeoproterozoic|Cleve-Coulta Domains, Gawler Craton.|c. 1850 Ma|||||
24194|Bosanquet Formation|71559|6|Mentioned|p15 Fig 1|Paleoproterozoic|Paleoproterozoic|Geological province: Gawler Craton.||||||
24194|Bosanquet Formation|71859|5|Briefly described|p4, p6|Orosirian|Orosirian|Cleve and Coulta domains, southern Gawler Craton.|c. 1850 Ma|Hutchison Group||||
24194|Bosanquet Formation|72090|6|Mentioned|p10|Orosirian|Orosirian|Cleve-Coulta Domain, Gawler Craton.|c. 1860 Ma|||||
24194|Bosanquet Formation|73026|6|Mentioned|p6|Paleoproterozoic|Paleoproterozoic|Central/western Eyre Peninsula.|c. 1875 Ma|||||
24194|Bosanquet Formation|73027|5|Briefly described|p6, p9|Palaeoproterozoic|Palaeoproterozoic|||||Overlies the Darke Peake Group.|Rhyodacite, recrystallised, interbedded with calcsilicate gneiss.|
24194|Bosanquet Formation|73030|6|Mentioned|p2149|Orosirian|Orosirian|Gawler Craton.||||||
24194|Bosanquet Formation|73104|6|Mentioned|p2||||||||Includes meta-igneous rocks.|
24194|Bosanquet Formation|73130|6|Mentioned|[poster] Fig.1|Paleoproterozoic|Paleoproterozoic|||||||28-OCT-22
24194|Bosanquet Formation|73234|6|Mentioned|p19|Orosirian|Orosirian|Eyre Peninsula, north-eastern. Gawler Craton. Age from Fanning, Reid and Teale (2007)[?].|c. 1865 Ma||||Metavolcanics.|
24194|Bosanquet Formation|73493|5|Briefly described|p716 Fig.3|||Gawler Craton.|||||Felsic volcanics, sandstone.|
24194|Bosanquet Formation|73525|5|Briefly described|p19 Fig.13|Orosirian|Orosirian|Cleve Domain.|1866+/-10 Ma, 1845+/-9 Ma|Darke Peak Group|||Felsic extrusives.|
23414|Box Bore Granite|22631|6|Mentioned|p176|Calymmian|Calymmian|||||||
23414|Box Bore Granite|24197|5|Briefly described|p75 Tb. 8.1|Mesoproterozoic|Mesoproterozoic|Age: 1560Ma.||||||07-FEB-11
23414|Box Bore Granite|42885|2|Defined|p26||Mesoproterozoic|see also Fig.3 p24.||||||17-JAN-19
23414|Box Bore Granite|43052|5|Briefly described|p153|||||||||
23414|Box Bore Granite|50605|5|Briefly described|p(iii), 1.4, 10.2, Table 1.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Gawler Craton & Curnamona Province. Of the Moolawatana Suite.||||||
23414|Box Bore Granite|62962|6|Mentioned|p2284 Fig. 2|Mesoproterozoic|Mesoproterozoic|Geological Province: Mount Painter Province.||||||07-FEB-11
23414|Box Bore Granite|65925|5|Briefly described|Appendix 2.||||||||Granite, coarse-grained, alkaline, potassic and foliated. With fluorite and allanite accessory minerals.|
23414|Box Bore Granite|66302|6|Mentioned|p49, p78|Calymmian|Calymmian|Ages are derived from Stewart and Foden (2003) and Fraser and Neumann (2010).|1560 Ma  to 1584 +/- 2 Ma |||||
23414|Box Bore Granite|67540|3|Fully described|p25; p27-28; p34,36,40 Tb.2,3,Fig.2|Calymmian|Calymmian|Type locality: W from Parabarana Hill towards the Brindana Gorge. Definition reference: Teale (1993), this article and Fricke and Hore (2011). Curnamona Province: Moolawatana Domain. Maximum age given here is by LA-ICP-MS (Kromkhun, 2010); the minimum is by SHRIMP (Fraser and Neumann, 2010).|1592 +/- 6 Ma to 1583 +/- 2 Ma.|Of the Coulthard Suite.||Faulted (thrust over) the Mount Neill Granite.|Typically pink to red and coarse grained (K-feldspar megacrysts to 5cm). Usually highly deformed. A-type.|
23414|Box Bore Granite|68068|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Curnamona Province.|c.1555 Ma (U-Pb zircon).|Unit in Moolawatana Suite.|||Coarse-grained (phenocrystic), alkaline, potassic granite, strongly foliated to mylonitic, red K-feldspar augen in melanocratic to leucocratic (often ribboned) groundmass; augen enwrapped by secondary biotite.|
23414|Box Bore Granite|69019|5|Briefly described|p27-29 Figs.7-9, p92 Fig.22.|||Geochemistry is described.||||Is overlain unconformably by Parabarana Sandstone.||
23414|Box Bore Granite|69023|5|Briefly described|p23-29, p34, p37-40, p43, p46, p49|||See also p53-54, p74, p98, p145, p162, p189, p202. Of Teale (1993). Previously included in Terrapinna Granite of Coats and Blissett (1971). Mount Babbage and Mount Painter Inliers. Geochemistry detailed. Exhibits Mesoproterozoic deeper crustal deformation: strong pervasive mylonitic fabric. Deep level emplacement. Where least deformed, it resembles Terrapinna Ganite. Age: concordia plot is discordant. Neumann et al. (2009) provide maximum crystallisation age of ~1585-1575 Ma. Red variant has potential as dimension stone.|1560 +/- 15 Ma U-Pb zircon (Fanning, 1995).|Unit in Moolawatana Suite.|||Very coarse-grained granite; protomylonitic to ultramylonitic with countless high strain bands; large reddish K-feldspar megacrysts enwrapped by recrystallised biotite; abundant grey quartz augen.|
23414|Box Bore Granite|69562|5|Briefly described|p670 Tb.5||||1583 +/- 2 Ma (Fraser and Neumann, 2010).|Unit in Coulthard Suite.|||Coarse-grained granite, gneissic fabric.|
23414|Box Bore Granite|69650|1|Redefined|p4 Tb.1, p8-9, p11, p13, p57-61, p64|Calymmian|Calymmian|See also p67-70, p73. Mapped by Campana et al. (1961). Defined by Teale (1993). Named for Box Bore, 15 km SE of Moolawatana Homestead. Type locality: can be seen cropping out along a station track west from Parabarana Hill towards the Brindana Gorge/Gunsight Prospect areas (Fig. 33) at GDA94, 371550 mE, 6681400 mN. Moolawatana Domain, Curnamona Province. Geochemistry discussed, and geochronology in some detail. Originally placed in Moolawatana Suite on the basis of early geochronology. Is included in Coulthard Suite on basis of similar chemical composition with unaltered Mount Neill Granite as well as age similarities.|1592-1583 Ma.|Unit in Coulthard Suite.||Is intruded by Mount Neill Granite. Is thrust over Mount Neill Granite. Is faulted against Brindana Schist.|Described as granitic gneiss or rapakivi granite and as augen-textured gneiss; typically pink to red, coarse-grained (K-feldspar megacrysts to 5cm); usually highly deformed. A-type.|25-NOV-22
23414|Box Bore Granite|70384|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Accessory minerals include fluorite, allanite, zircon and monazite. SHRIMP U-Pb zircon ages. Another age given is 1586 +/- 45 Ma (ICPMS).|1555 +/- 15 Ma; 1585 +/- 3 Ma.|Coulthard Suite.|||Coarse-grained (porphyritic) alkaline, potassic granite, strongly foliated to mylonitic, red K-feldspar augen in melanocratic to leucocratic (often ribboned) groundmass. Augen enwrapped in secondary biotite.|
23414|Box Bore Granite|70658|5|Briefly described|p33-35|Mesoproterozoic|Mesoproterozoic|Mount Painter Inlier, Curnamona Province. Geochemistry briefly described. Outcrop area c.20 km2.|1592-1583 Ma.|Coulthard Suite.|||Typically pink to red, coarse-grained, K-feldspar megacrysts up to 5cm, rapakivi texture. Usually highly deformed. A-type.|
23414|Box Bore Granite|72949|6|Mentioned|p36|Calymmian|Calymmian|Curnamona Province. Mount Painter.|1592-1583 Ma|||||
23414|Box Bore Granite|73061|5|Briefly described|p1067, p1070 Tb.1, p1071-1072, p1076|Calymmian|Calymmian|Mount Painter Province. High heat producing granite. Mean eHf value of +0.8 +/- 0.5. Could possibly be a strongly deformed zone of the Mount Neill Granite based on similar ages. Location in text includes p1069 Fig.1, p1074 Fig.4.|1580 +/- 21 Ma U-Pb LA-ICPMS, 1583 +/- 2 Ma||||Includes pink, gneissic granite with rounded coarse-grained feldspar phenocrysts.|
28396|Brachina Formation|7931|5|Briefly described|p98, p99 Fig. 2|Ediacaran|Ediacaran|Of Sandison Subgroup (Wilpena Group). Overlies the Nucculeena Formation; underlies ABC Range Quartzite. Shelf deposits of thick shales and sandstones.||||||07-FEB-11
28396|Brachina Formation|9862|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Probably of the Wilpena Group. Green silty slates.||||||
28396|Brachina Formation|22570|5|Briefly described|p197|Neoproterozoic|Neoproterozoic|||||||
28396|Brachina Formation|22631|6|Mentioned|p178|||Age: Marianoan||||||
28396|Brachina Formation|22646|6|Mentioned|Fig 4 on p 102|Neoproterozoic|Neoproterozoic|Adelaide Geosyncline (West).  Age - Ediacarian in text.||||||
28396|Brachina Formation|22649|6|Mentioned|p 143|||Rb-Sr age 676+/-204 Ma p 143.  Province - Adelaide Geosyncline.||||||
28396|Brachina Formation|22677|5|Briefly described|p734|Neoproterozoic|Neoproterozoic|||||||
28396|Brachina Formation|22746|6|Mentioned|p528|||||||||
28396|Brachina Formation|22857|5|Briefly described|p93|||Age: 536+/-7Ma (Rb/Sr, Turner, Sandiford et al, 1994).||||||
28396|Brachina Formation|22858|5|Briefly described|p93||Early Cambrian| Age of cleavage formation: 536 (+/-) 7 Ma.||||||16-AUG-18
28396|Brachina Formation|22901|6|Mentioned|78|||Geol province Adelaide Rift Complex||||||
28396|Brachina Formation|22921|6|Mentioned|37|||Parent Wilpena Group||||||
28396|Brachina Formation|22927|5|Briefly described|40|||Geol Province: Adelaide Geosyncline.||||||13-FEB-08
28396|Brachina Formation|23023|6|Mentioned|p1797,1799|||||||||
28396|Brachina Formation|23180|6|Mentioned|p35, Fig.2|||||||||
28396|Brachina Formation|23211|5|Briefly described|p41,45 Fig.2|||Of Sandison Subgroup.||||||13-FEB-08
28396|Brachina Formation|23250|5|Briefly described|p1124 Fig.2||Neoproterozoic III|Of Wilpena Group. Correlate of Tent Hill Formation, Gayland Sandstone, Waldo Pedlar Member, Cyclops Member and Pertatataka Formation.||||||13-FEB-08
28396|Brachina Formation|23287|6|Mentioned|p104 Fig.2-4|||Age: Lower Ediacarian. Adelaide Geosyncline.||||||
28396|Brachina Formation|23315|5|Briefly described|p345|Neoproterozoic|Neoproterozoic|Of the Wilpena Group. Finely laminated dolomite, siltstone.||||||13-FEB-08
28396|Brachina Formation|23445|5|Briefly described|p435|Neoproterozoic|Neoproterozoic|Of Wilpena Group, 609+/-64Ma.||||||13-FEB-08
28396|Brachina Formation|23562|5|Briefly described|p295 Fig 2|Neoproterozoic III|Neoproterozoic III|||||||
28396|Brachina Formation|23719|5|Briefly described|p25 Taable 7|||See also page 26. Of Wilpena Group. O'lying unit ABC Range Quartzite. U'lying unit Seacliff Sandstone. Geological Province: Gawler Craton. Max. thickness: >160 m.||||||
28396|Brachina Formation|23806|5|Briefly described|p1122 Fig. 1|Neoproterozoic|Neoproterozoic|||||||
28396|Brachina Formation|23818|5|Briefly described|p73 Fig.27, p75|Adelaidean|Adelaidean|Of the Wilpena Group. Max. thickness: 4000 ft. Has ripple marks and heavy mineral layering. Overlying unit: ABC Range Quartzite.||||||
28396|Brachina Formation|23913|4|Described|p108, p110 Fig. 2|Adelaidean|Adelaidean|Geological Province: Central Flinders Zone. Of the Wilpena Group.  Age: 601 +/- 68 Ma. Underlying Unit: Nuccaleena Formation. Overlying Unit: ABC Range Quartzite.||||||13-FEB-08
28396|Brachina Formation|24175|4|Described|p13|Neoproterozoic|Neoproterozoic|Of the Wilpena Group. Overlain by Bunyeroo Formation; overlies Nuccaleena Formation. Max. thickness: 1015m.||||||13-FEB-08
28396|Brachina Formation|24176|4|Described|p14, p24 Tb. 1|Adelaidean|Adelaidean|Of the Wilpena Group. Siltstones, shales, minor sandstones. Intertongues with ABC Range Quartzite. Overlies the Nuccaleena Formation.  Age is Marinoan.  Max. thickness: 2745m.  Geological Province: Mount Painter Province. See also p27 Tb. 2.||||||13-FEB-08
28396|Brachina Formation|24195|5|Briefly described|p45 Fig.3|||Max Thickness: ~700m at Hallet Cove. Geological Province: Adelaide Geosyncline.||||||13-FEB-08
28396|Brachina Formation|24321|5|Briefly described|Map legend|Late Adelaidean|Late Adelaidean|Parent: Wilpena Group.||||||13-FEB-08
28396|Brachina Formation|24476|4|Described|p547 Fig. 4|Vendian|Vendian|Overlies the Nuccaleena Formation. Overlain by the ABC Range Quartzite. Geological Province: Adelaide fold belt.||||||
28396|Brachina Formation|24586|5|Briefly described|p51 Fig. 2, p52 Fig. 3|Adelaidean|Adelaidean|Of the Sandison Subgroup ((Wilpena Group). Onlaps brecciated dolostone of Nuccaleena Formation.  Geological Province: Adelaide Geosyncline.||||||
28396|Brachina Formation|29780|4|Described|p42|||||||||
28396|Brachina Formation|29834|6|Mentioned|p198|||||||||
28396|Brachina Formation|30176|6|Mentioned|Map legend|Adelaidean|Adelaidean|Marinoan||||||
28396|Brachina Formation|30198|6|Mentioned|p96|||See also Table 2 for lithology. Refers to aquifers||||||
28396|Brachina Formation|30801|6|Mentioned|p5|||Marinoan. Table P5-6||||||
28396|Brachina Formation|30802|5|Briefly described|p12|||Marinoan.||||||
28396|Brachina Formation|30807|6|Mentioned|p102|||Suggested map symbol||||||
28396|Brachina Formation|31797|6|Mentioned|Fig. 2|||Adelaidean||||||
28396|Brachina Formation|31923|6|Mentioned|p10|||||||||
28396|Brachina Formation|32144|6|Mentioned|p81|||Organic matter||||||
28396|Brachina Formation|32146|6|Mentioned|Fig.3|||||||||
28396|Brachina Formation|32504|6|Mentioned|Fig.2|||||||||
28396|Brachina Formation|32505|6|Mentioned|Table 3|||||||||
28396|Brachina Formation|32506|6|Mentioned|Fig.1|||||||||
28396|Brachina Formation|32511|6|Mentioned|p13|||Host to extensive barite lodes.||||||13-FEB-08
28396|Brachina Formation|32720|6|Mentioned|Table 1|||||||||
28396|Brachina Formation|32722|6|Mentioned|Fig.3|||Adelaidean. Stromatolite.||||||13-FEB-08
28396|Brachina Formation|32724|6|Mentioned|Fig.1|||Marinoan. Correlation.||||||13-FEB-08
28396|Brachina Formation|33036|6|Mentioned|p18|||||||||
28396|Brachina Formation|33037|6|Mentioned|Fig.2|||||||||
28396|Brachina Formation|33224|6|Mentioned|p40|||Refers barite deposits.||||||13-FEB-08
28396|Brachina Formation|33423|6|Mentioned|p13|||||||||
28396|Brachina Formation|33474|6|Mentioned|Fig.3|||||||||
28396|Brachina Formation|33729|6|Mentioned|p82|||Fauna.||||||
28396|Brachina Formation|34116|6|Mentioned|p20|||||||||
28396|Brachina Formation|34175|6|Mentioned|p36|||||||||
28396|Brachina Formation|34201|6|Mentioned|p376|||Fauna||||||
28396|Brachina Formation|34267|6|Mentioned|Fig.|||The Oraparinna & Enorama diapiric structures.||||||
28396|Brachina Formation|34268|6|Mentioned|p241|||U.Prot.||||||
28396|Brachina Formation|34269|6|Mentioned|Table 1|||||||||
28396|Brachina Formation|34291|5|Briefly described|p18|||See also PP19,20,41 etc. Adelaidean.||||||13-FEB-08
28396|Brachina Formation|34521|5|Briefly described|p156|||Suitability for road-making||||||
28396|Brachina Formation|34534|6|Mentioned|Fig.2.13|||||||||
28396|Brachina Formation|34535|5|Briefly described|p74|||Fig.27||||||
28396|Brachina Formation|34563|6|Mentioned|p67|||Correlation||||||
28396|Brachina Formation|34612|6|Mentioned|Fig.55|||||||||
28396|Brachina Formation|34835|6|Mentioned|Fig.2|||||||||
28396|Brachina Formation|34836|6|Mentioned|Fig.2|||||||||
28396|Brachina Formation|34844|6|Mentioned|Fig.2|||||||||
28396|Brachina Formation|35002|6|Mentioned|p28|||||||||
28396|Brachina Formation|35075|6|Mentioned|Fig.2|||||||||
28396|Brachina Formation|35143|6|Mentioned|Fig.2|||||||||
28396|Brachina Formation|35158|6|Mentioned|p47|||||||||
28396|Brachina Formation|35195|6|Mentioned|Table 3|||||||||
28396|Brachina Formation|35255|6|Mentioned|Fig.3|||||||||
28396|Brachina Formation|35356|6|Mentioned|p30|||||||||
28396|Brachina Formation|35582|6|Mentioned|Fig.2|||||||||
28396|Brachina Formation|35586|6|Mentioned|p25|||||||||
28396|Brachina Formation|35678|6|Mentioned|Fig.2|||Geological cross-sections, northern Yorke Peninsula.||||||
28396|Brachina Formation|36137|4|Described|p17|||See also p6.||||||16-AUG-18
28396|Brachina Formation|36198|6|Mentioned|p279|||||||||
28396|Brachina Formation|36245|6|Mentioned|Fig.1|||||||||
28396|Brachina Formation|36621|6|Mentioned|Fig.1|||||||||
28396|Brachina Formation|36731|6|Mentioned|p122|||Fig.3||||||
28396|Brachina Formation|36898|6|Mentioned|p197|||||||||
28396|Brachina Formation|37461|6|Mentioned|Table 5.I|||||||||
28396|Brachina Formation|38022|6|Mentioned|Fig.4|||||||||
28396|Brachina Formation|38110|6|Mentioned|p2|||||||||
28396|Brachina Formation|38157|6|Mentioned|Table 1|||Also mentioned in Table V.||||||
28396|Brachina Formation|38330|6|Mentioned|p217|||||||||
28396|Brachina Formation|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Marinoan||||||
28396|Brachina Formation|39349|6|Mentioned|Map legend|Adelaidean|Adelaidean|Marinoan||||||
28396|Brachina Formation|39351|6|Mentioned|Map legend|Adelaidean|Adelaidean|Marinoan||||||
28396|Brachina Formation|39352|6|Mentioned|Map legend|Adelaidean|Adelaidean|Marinoan||||||
28396|Brachina Formation|39526|6|Mentioned|Fig.2|||||||||
28396|Brachina Formation|39675|6|Mentioned|Fig.2|||||||||
28396|Brachina Formation|39808|6|Mentioned|p223|||||||||
28396|Brachina Formation|40228|5|Briefly described|p38|||||||||
28396|Brachina Formation|40254|6|Mentioned|p284|||||||||
28396|Brachina Formation|40442|5|Briefly described|Fig.4|||Mention on P10.||||||
28396|Brachina Formation|40448|5|Briefly described|p38|||||||||
28396|Brachina Formation|40720|5|Briefly described|p55|||||||||
28396|Brachina Formation|40914|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
28396|Brachina Formation|41005|6|Mentioned|p418|||||||||
28396|Brachina Formation|41236|5|Briefly described|p63|||||||||
28396|Brachina Formation|41401|6|Mentioned|p33|||||||||
28396|Brachina Formation|41429|3|Fully described|p120|||||||||
28396|Brachina Formation|41494|5|Briefly described|p34|||||||||
28396|Brachina Formation|41496|5|Briefly described|Fig.1|||||||||
28396|Brachina Formation|41526|6|Mentioned|p27|||||||||
28396|Brachina Formation|41794|6|Mentioned|p780|||||||||
28396|Brachina Formation|41801|6|Mentioned|Fig.4|||||||||
28396|Brachina Formation|42028|6|Mentioned|p137|||||||||
28396|Brachina Formation|42090|5|Briefly described|p25|||||||||
28396|Brachina Formation|42100|6|Mentioned|p70|||||||||
28396|Brachina Formation|42222|6|Mentioned|Table 1 P4|||||||||
28396|Brachina Formation|42235|4|Described|p140|||See also Fig.3||||||
28396|Brachina Formation|42238|5|Briefly described|p77|||||||||
28396|Brachina Formation|42239|5|Briefly described|p160|||||||||
28396|Brachina Formation|42241|5|Briefly described|p178|||||||||
28396|Brachina Formation|42272|5|Briefly described|p403|||||||||
28396|Brachina Formation|42375|6|Mentioned|Fig. 29 P129|||Precambrian||||||
28396|Brachina Formation|42410|6|Mentioned|p3|||||||||
28396|Brachina Formation|42498|5|Briefly described|Map Legend|Adelaidean|Adelaidean|||||||
28396|Brachina Formation|42505|5|Briefly described|Map legend|Adelaidean (Marinoan)||||||||
28396|Brachina Formation|42542|6|Mentioned|p14|||||||||
28396|Brachina Formation|42546|5|Briefly described|Map legend|Adelaidean (Marinoan)||||||||
28396|Brachina Formation|42600|4|Described|p9|||||||||
28396|Brachina Formation|42736|5|Briefly described|map legend|Neoproterozoic||||||||
28396|Brachina Formation|42763|5|Briefly described|Fig.3 P23|||||||||
28396|Brachina Formation|42779|6|Mentioned|p286|||||||||
28396|Brachina Formation|42813|6|Mentioned|p22|||||||||
28396|Brachina Formation|42882|5|Briefly described|Fig.7 P12|||Of Wilpena Group.||||||13-FEB-08
28396|Brachina Formation|43011|6|Mentioned|Table 2,p12|||||||||
28396|Brachina Formation|43052|5|Briefly described|p192,table 6.1|||Of Wilpena Group.||||||13-FEB-08
28396|Brachina Formation|43094|5|Briefly described|p36|||||||||
28396|Brachina Formation|43595|5|Briefly described|p547|||||||||
28396|Brachina Formation|43622|6|Mentioned|p38|Neoproterozoic||||||||
28396|Brachina Formation|43845|5|Briefly described|Fig3 p43, 46||Neoproterozoic|In Wilpena Group.||||||12-JUL-16
28396|Brachina Formation|44133|5|Briefly described|p23, 68|Precambrian|Precambrian|Disconformably underlies: Wilkawillina Limestone.||||||
28396|Brachina Formation|44659|5|Briefly described|map legend|||Marinoan, lithology.||||||
28396|Brachina Formation|44660|14|Not recorded|map legend|||Marinoan, lithology.||||||
28396|Brachina Formation|44689|14|Not recorded|map legend|||Marinoan. Andamooka (H53-12).||||||
28396|Brachina Formation|46865|6|Mentioned|Table 2|||||||||
28396|Brachina Formation|50127|6|Mentioned|p48 Fig.2|||Geological Province: Stuart Shelf.||||||
28396|Brachina Formation|50327|6|Mentioned|p308|||In the Flinders Ranges.||||||07-FEB-11
28396|Brachina Formation|60718|5|Briefly described|p49 Fig. 2|Adelaidean|Adelaidean|Geological Province: Adelaide Geosyncline. See also p51 Fig. 3.||Of Sandison Subgroup (Wilpena Group).||||15-APR-11
28396|Brachina Formation|60889|6|Mentioned|p250 Fig.7|Neoproterozoic|Neoproterozoic|||||||
28396|Brachina Formation|60955|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Wilpena Group. Green and purple micaceous siltstones.||||||
28396|Brachina Formation|60959|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Of the Sandison Subgroup. Red-brown and grey-green siltstone and sandstone.||||||
28396|Brachina Formation|61236|6|Mentioned|p24 Fig. 1|Adelaidean|Adelaidean|||||||
28396|Brachina Formation|61308|5|Briefly described|p7|Proterozoic|Proterozoic|Shale and sandstone.||||||
28396|Brachina Formation|61565|5|Briefly described|p609 Fig. 3|Neoproterozoic III|Neoproterozoic III|Geological Province: Adelaide Fold Belt.||||||
28396|Brachina Formation|61732|3|Fully described|p5 Tb. 1, p42-43|Marinoan|Marinoan|Of Sandison Subgroup (Wilpena Group). Includes Moolooloo Siltst, Moorillah Siltst + Bayley Range Siltst Mbrs. Gradational contact with Nuccaleena Fm below; conformably overlain by ABC Quartzite. Thick: >1200m. See also p150.||||||07-FEB-11
28396|Brachina Formation|62085|6|Mentioned|p18, p20 fig 5, p21 fig 6 |Ediacaran|Ediacaran|||Wilpena Group||Overlies Nuccaleena Formation.|Post-glacial siltstone, sandstone.|
28396|Brachina Formation|62428|5|Briefly described|p351 Tb. 6|Early Cambrian|Neoproterozoic III|Palaeomagnetic data.||||||10-FEB-09
28396|Brachina Formation|62592|5|Briefly described|p50 Table 5.1, p59.|Ediacaran|Ediacaran|Adelaide Geosyncline.||Unit in Sandison Subgroup.||Overlies Nuccaleena Formation. Is overlain by ABC Range Quartzite.|Grey-green siltstone, sandstone.|
28396|Brachina Formation|62903|5|Briefly described|p729, p730 Fig.1|Marinoan|Marinoan|Adelaide Rift Complex. Postglacial. Age from McKirdy et al. 2001.|601+/-68 Ma, Rb-Sr whole rock shale|||overlies Nuccaleena Formation; ia overlain by ABC Range Quartzite||
28396|Brachina Formation|63458|6|Mentioned|p897 Fig.19. |Ediacaran|Ediacaran|||Unit in Wilpena Group.||||
28396|Brachina Formation|63811|6|Mentioned|P506|||||Of the Adelaide Rift Complex.||||28-MAR-12
28396|Brachina Formation|64400|5|Briefly described|p6|||Of the Wilpena Group in the Adelaide Rift Complex.||||||07-FEB-11
28396|Brachina Formation|64455|5|Briefly described|p138 Fig. 1|Ediacaran|Cryogenian|Of Sandison Subgroup. Includes Moolooloo Siltstone Member, Moorillah Siltstone Member and Bailey Range Siltstone Member. Overlian by ABC Range Quartzite.||||||29-JAN-09
28396|Brachina Formation|64797|5|Briefly described|p152, p153 Fig.2, p161, p164 Figs.10-11 |Ediacaran|Ediacaran|See also p167 Tb.9 and 10, p168 Tb.11, p169 Fig.12, p176-177. Adelaide Rift Complex. S-isotope data. International correlations.|580 Ma.|Wilpena Group||Correlated with Pertatataka Formation of Amadeus Basin.||
28396|Brachina Formation|64801|6|Mentioned|p112|Neoproterozoic|Neoproterozoic|||||||
28396|Brachina Formation|64829|5|Briefly described|p1084 Fig. 1|Neoproterozoic|Neoproterozoic|||||||07-FEB-11
28396|Brachina Formation|65313|6|Mentioned|p576 Fig. 5|Neoproterozoic|Neoproterozoic|||||||
28396|Brachina Formation|65338|6|Mentioned|p64.|||Adelaide Fold Belt. Correlated with Elyuah Formation.||||||
28396|Brachina Formation|65410|6|Mentioned|p74.|||Adelaide Geosyncline. Part of Supersequence 3.||||||
28396|Brachina Formation|65644|6|Mentioned|p5,18|Neoproterozoic|Neoproterozoic|Of the Adelaide Geosyncline. Correlated with Yarra Creek Shale, King Island. Age: Marinoan.|||||Includes black shales composed of benthic microbial mats.|27-MAR-12
28396|Brachina Formation|65664|6|Mentioned|p1106 Fig.5|||||Of Wilpena Group.||||09-MAY-12
28396|Brachina Formation|65892|4|Described|p32-33, p35, p37-39.  |Ediacaran|Ediacaran|Adelaide Geosyncline. Is equivalent to Meramangye Formation in the eastern Officer Basin.|c.600 Ma.|Unit in Wilpena Group.||Overlies Nuccaleena Formation. Is overlain by ABC Range Quartzite.|Red-brown siltstones and shales; minor sandstone.|
28396|Brachina Formation|65925|5|Briefly described|Appendix 2.||||||||Siltstone, shale, red-brown and olive green, laminated, flaggy to medium bedded; alternating with sandstone, fine grained, occasionally coarse grained. All lithologies calcitic in part.|
28396|Brachina Formation|66464|6|Mentioned|p167, p169 Fig.3, p171-173 Figs.5-8|Ediacaran|Ediacaran|Adelaide Rift Complex. Overlies Nuccaleena Formation.||||||
28396|Brachina Formation|66569|4|Described|p860, p861 fig.2, p861,|Ediacaran|Ediacaran|Of Wilpena Group; intertongues with Seacliff Sandstone; overlies Nuccaleena Formation; underlies ABC Range Quartzite; red-brown and minor olive green siltstone and mudstone and local sandstone; Rb-Sr isochron of 609+/-64 Ma; equivalent to Woomera Shale.||||||
28396|Brachina Formation|67030|5|Briefly described|p407-9, p412 Fig.7, p413 Tab. 2|Ediacaran|Ediacaran|Age of 609 +/- 64 Ma (Rb-Sr, Compston et al. 1987) with a best estimate of ~590 Ma. Abrrev as Brachina Fm Tb. 2. Magnetic information presented for comparison (Schmidt & Williams 2010).|590 Ma||Bayley Range, Moorillah and Moolooloo, Siltstone Members.|Overlain by ABC Quartzite, underlain by Nuccaleena Formation; equivalent to the Ulupa Siltstone.||26-APR-12
28396|Brachina Formation|67484|6|Mentioned|p294 Tb.1, p296|Ediacaran|Ediacaran|Adelaide Rift Complex.||Of the Wilpena Group.||Overlain by ABC Range Quartzite. Underlain by Nuccaleena Formation.||
28396|Brachina Formation|67620|5|Briefly described|p5, 22|Ediacaran|Ediacaran|Adelaide Rift Complex. Contains abundant organic laminae (microbial mats).||Wilpena Group.||Overlies Nuccaleena Formation (Umberatana Group). Is overlain by ABC Range Quartzite.||
28396|Brachina Formation|67870|5|Briefly described|p9|Ediacaran|Ediacaran|Adelaide Rift System.||Sandison Subgroup.||||
28396|Brachina Formation|68030|4|Described|p237-239|Ediacaran|Ediacaran|Flinders Ranges. Over 1.3km thick sequence of upward shallowing and coarsening regressive siliciclastics. Correlated with the Ulupa Siltstone to the N and E. Upward-shoaling Brachina Fm and ABC Range Qtz represent a HST of progradatioal siliciclastics from Gawler Craton into Andelaide Geosyncline.||Unit of Wilpena Group.||Overlain/grades upwards into ABC Range Quartzite. Underlain by Nuccaleena Formation.|Rhythmically bedded laminated siltstones grade up into silty, cross-laminated fine-grained sandstones.|26-JUN-19
28396|Brachina Formation|68138|6|Mentioned|p156|Neoproterozoic|Neoproterozoic|Adelaide Rift Complex.||Wilpena Group.||||
28396|Brachina Formation|68241|6|Mentioned|p24 Fig.3, p33 Fig.3|||~ 1000m thick.|||||Dolomite.|
28396|Brachina Formation|68243|6|Mentioned|p651|||||||||
28396|Brachina Formation|68269|6|Mentioned|p674|||Adelaide Geosyncline.||Wilpena Group||Underlain by Nuccaleena Formation. Overlain by ABC Range Quartzite.|Siltstone dominated.|
28396|Brachina Formation|68275|6|Mentioned|p59|||||||Overlies Nuccaleena Formation.||
28396|Brachina Formation|68276|6|Mentioned|p73|||||||Shales, siltstones and sandstones overlie cap dolostones.||
28396|Brachina Formation|68473|6|Mentioned|p531|||Adelaide Rift Complex.||||||
28396|Brachina Formation|69017|6|Mentioned|p96-97|||||||Overlies Nuccaleena Formation.|A thick (>800m) succession of upward-shoaling siltstone and minor sandstone. Dolostone interbedded with red siltstone.|
28396|Brachina Formation|69019|5|Briefly described|p54-55.|Neoproterozoic|Neoproterozoic|Ulupa Siltstone is considered (Preiss, 1993) to be a distal equivalent of this unit.||Unit in Sandison Subgroup.||Equivalent to Ulupa Siltstone.|Red-brown to olive-green siltstone to sandstone.|
28396|Brachina Formation|69841|6|Mentioned|p19|Ediacaran|Ediacaran|||||Lower part is correlated with Yarra Creek Shale.||
28396|Brachina Formation|70031|5|Briefly described|p245,250-251|Ediacaran|Ediacaran|Adelaide Geosyncline. Ca. 610 Ma date for late Cryogenian to post-Delamerian Orogeny poles. See p250 Table 2 for paleomagnetic analysis.||Unit of Wilpena Group.||Overlain by ABC Range Quartzite. Underlain by Nuccaleena Formation.||
28396|Brachina Formation|70082|5|Briefly described|p2-5,15-16|Ediacaran|Ediacaran|Flinders Ranges and Kulpara-Adelaide region. Contains red beds. Preserves evidence of Delamerian deformation; gently folded in Marino Anticline, with Rb-Sr dating of sericite in cleavage at 531+\-32 Ma (Early Cambrian) (Turner et al., 1994; Preiss et al., 1995). Contains thin clay seams metamorphosed to lower greenschist facies (Turner et al., 1994; Preiss et al., 1995). Records post-glacial marine transgression, indicative by gray sltstones and hummocky cross bedding. Also does not contain dropstones or evidence of sea ice or ice bergs (Dyson, 1983, 2002; Dyson and von der Borch, 1994).|||Includes Seacliff Sandstone Member.|Underlain by Reynella Siltstone Member.||
28396|Brachina Formation|70323|6|Mentioned|p221|||Adelaide Geosyncline. Contains moderately iron-oxide-rich sediments.||||||
28396|Brachina Formation|70333|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic||||||Siltstone, shale, red-brown and olive-green, laminated, flaggy to medium-bedded; alternating with sandstone, fine-grained, occasionally coarse-grained. All lithologies calcitic in part.|
28396|Brachina Formation|70334|4|Described|p2,20,33-34,57,65,77,79,81|Ediacaran|Ediacaran|Geological province: Gawler Craton. Of Adelaide Geosyncline. Highstand systems tract, representing rapid marine transgression during interglacial period after Sturtian glaciation over the Stuart Shelf. Deformed by Cambrian-Ordovician Delamarian Orogeny (~515-480 Ma). Thickness variation is a result of reactivation of the Torrens Hinge Zone, resulting in rapid increase in thickness on the eastern side of faults. Equivalent to Corraberra Sandstone Member or Moolooloo Siltstone Member.||Unit of Sandison Subgroup.||Overlain by ABC Range Quartzite. Underlain by Seacliff Sandstone. Equivalent to Tent Hill Formation.|Dominantly chocolate-brown siltstone containing laminae and interbeds of red-brown to grey-green sandstone.|
28396|Brachina Formation|70406|5|Briefly described|p126, p122, 123, 124, 125, 127, 128, 117|Neoproterozoic|Neoproterozoic|||Of Sandison Subgroup.|Said to consist of 4 members: Bayley Range Siltstone, Corraberra Sandstone Member, Moolooloo Siltstone Member, Moorillah Siltstone Member.|Correlated with Tent Hill Formation.||09-MAY-16
28396|Brachina Formation|70407|5|Briefly described|p103 Fig 2, 105|Neoproterozoic|Neoproterozoic|Age: Marinoan.||Of Sandison Subgroup, Wilpena Group.|Includes Moolooloo, Moorilah and Bayley Range Siltstone Members.|||
28396|Brachina Formation|70790|6|Mentioned|p258 Fig.1|Ediacaran|Ediacaran|Adelaide Rift Complex.||||||
28396|Brachina Formation|71129|5|Briefly described|p128-129,131|Ediacaran|Ediacaran|Of Adelaide Geosyncline.||Unit of Sandison Subgroup.|Includes Bayley Range Siltstone Member, Moorillah Siltstone Member and Moolooloo Member.|Broadly equivalent to Tent Hill Formation.||
28396|Brachina Formation|71237|14|Not recorded|p9, 10, 17|||||||||
28396|Brachina Formation|71241|2|Defined|p13,14, 17, p9-10|||||Of Wilpena Group.||Conformably overlies Nuccalena Formation.||
28396|Brachina Formation|71242|6|Mentioned|p9, 10, 11|||||||||
28396|Brachina Formation|71250|6|Mentioned|p70|Ediacaran|Ediacaran|Central Flinders Ranges.||Wilpena Group.||Overlies Nuccaleena Formation. Is overlain by ABC Range Quartzite.||
28396|Brachina Formation|72429|6|Mentioned|p958, p972|Neoproterozoic|Neoproterozoic|Intersected in Moorowie 1 petroleum exploration well at a depth of 2228m, alongside the Brillig Catch Member, 11.5km east of the Moorowie Mine.||Wilpena Group||||
28396|Brachina Formation|72449|5|Briefly described|p1, p2 Map Legend|Neoproterozoic|Neoproterozoic|Shallow marine.||||Overlies Nuccaleena Formation and underlies ABC Range Quartzite.|Upper: Olive-green silts tone, coarsening upwards to ripple-marked and cross bedded sandstone. Middle: Reddish. Coarse-grained banded siltstone. Lower: Drab olive-green to brown mica-rich siltstone.|
28396|Brachina Formation|72450|5|Briefly described|Brochure, Brochure map|||Present as sea cliffs between Hallett Cove and O'Sullivan Beach. Deformed by the Delamerian Orogeny. Striated by Permian glaciation.||Wilpena Group||Underlies the ABC Range Quartzite.|Thinly bedded red siltstone with red sandstone at the top.|
28396|Brachina Formation|72451|4|Described|p4|Late Proterozoic|Late Proterozoic|Informally referred to as Pencil shale, due to highly fractured and regular jointed nature. Depositional environment: very low energy. May represent distal margin of the proximal deltaic ABC Range quartzite.|||||Red-brown and olive-green siltstone, grading in places to shale and flaggy fine sandstone.|
28396|Brachina Formation|72473|6|Mentioned|p4|||||||||
28396|Brachina Formation|73086|6|Mentioned|p122|||Adelaide Rift Complex.||||Correlates to Pertatataka Formation.||
28396|Brachina Formation|73110|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic||||||Siltstone, shale, red-brown and olive-green, laminated, flaggy to medium-bedded; alternating with sandstone, fine-grained, occasionally coarse-grained. All lithologies calcitic in part.|
28396|Brachina Formation|73188|5|Briefly described|p316, p326, p331, p335|Ediacaran|Ediacaran|Mount Lofty Ranges.||Sandison Subgroup, Wilpena Group|||Red-brown and grey-green siltstone.|
28396|Brachina Formation|73222|6|Mentioned|p6, p11, p16, p23-24, p26|Ediacaran|Ediacaran|Adelaide Rift Complex.||Sandison Subgroup, Wilpena Group, Heysen Supergroup||||
28396|Brachina Formation|73236|4|Described|p36-40, p44-47|Ediacaran|Ediacaran|Marine (outer continental) shelf sedimentary rocks. Post-glacial. Interbedded, fine-grained sandstone beds display flute casts; interpreted as storm-modified turbidites. Responded to the compressive stresses of the Delamerian Orogeny by forming tight, chevron-style folds as seen at Black Cliff. Slickensided surfaces indicate bedding-plane slip during folding. Slaty cleavage is developed in the fine-grained siltstones at Hallett Cove. Gradational base. Represents high-stand deposits.||Sandison Subgroup, Wilpena Group, Heysen Supergroup||Conformably underlain by Nuccaleena Formation. Overlain by ABC Range Quartzite.|Dark red-brown and grey-green, well-bedded siltstone, minor fine-grained dolomite with red shale partings.|
28396|Brachina Formation|73255|6|Mentioned|p534 Fig.2|Ediacaran|Ediacaran|Contains Bunyerichnus dalgarnoi fossils.||||Overlies the Nuccaleena Formation, underlies the ABC Quartzite.||
28396|Brachina Formation|74367|5|Briefly described|p7 Fig.6, p8, p11, p19-20, p22|Ediacaran|Ediacaran||609+/-64 Ma Rb-Sr LA-ICP-MS detrital zircon MDA|Sandison Subgroup||||
79317|Branson Well Quartzite|71416|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Metamorphosed c.1170 Ma. SHRIMP U-Pb zircon ages by Jagodzinski et al. (in prep.).|c.1550 Ma (protolith maximum deposition age).||||Quartzite, pale grey, quartz with minor feldspar, sillimanite, magnetite and garnet.|
70230|Breakfast Time Creek Member|64460|5|Briefly described|p197, p198, p208|||Of Rawnsley Quartzite (a new member). Thickness: 34m. Also a misspelling on p208 (Breakfast Time Greek Member).||||||23-AUG-18
28398|Breckan Sand|29425|6|Mentioned|p104|||||||||
28398|Breckan Sand|65901|6|Mentioned|p176 Tab.1, p177|||Of Bourman (1968). Equivalent to Waldeila Formation.||||||08-MAR-12
76217|Brillig Catch Member|72429|3|Fully described|p952, p956, p971-972|Lower Cambrian|Lower Cambrian|Mount Chambers Gorge, eastern Flinders Ranges. Forms a single laterally continuious and consistent blanket up to 41m thick in measured section. Layers range from fine book-like lamellae of microbial character up to 300mm thick flagstones, all seperated by thin argillaceous partings. Features a very low content of siliciclastic material, with subtle reworking of the beds by gentle currents indicated by clay wisps, silt and occasional limestone intraclasts. Accessories may include black chert granules, dusty hematite and limonite. Prominent karren weathering surfaces and stylolites are present; other textures discussed. Interpreted to have been deposited in an extensive, low-energy, evaporitic, restricted and protected intertidal estuarine sabkha environment passing into supratidal continental sabkhas. Interpreted therefore to have been intersected in Moorowie 1 petroleum drill hole, 11.5km east of the Moorowie Mine. At the top of this unit is a very persistent marker bed, 3-7m thick consisting of flat sheets of light grey, micro-crystalline syngenetic dolostone or limestone, separated by equally thin, khaki-green, argillaceous partings. A protected shallow, evaporitic, intertidal to supratidal sabkha is indicated by this bed. The succession continues above the marker bed with a laterally variable bed, 150mm thick of dolostone and peloidal limestone that is discussed further. This bed shows there was minor reworking of dolomitic horizons.||Moorowie Formation||Underlies the Billy Creek Formation. Overlies the Pack Creek Member. Potentially equivalent to the Edeowie Limestone Member.|Medium-grey, uniformly very-fine grained, lean, massive, homogeneous, flaggy to medium-bedded, microbial limestone to dolostone with thin shale partings. Possibly sideritic in part; no obvious macrofossils.|
25811|Brindana Schist|23394|5|Briefly described|Map legend|Proterozoic|Proterozoic|||||||
25811|Brindana Schist|23411|6|Mentioned|Map Legend|||||||||
25811|Brindana Schist|23818|5|Briefly described|p35|Proterozoic|Proterozoic|Of the Radium Creek Metamorphics.||||||
25811|Brindana Schist|24176|4|Described|p7, p26 Tb. 1|Proterozoic|Proterozoic|Of Radium Creek Metamorphics.  Muscovite schists, minor garnet schists.  Max. thickness: >950m.  Geological Province: Mount Painter Province.||||||
25811|Brindana Schist|30176|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
25811|Brindana Schist|30177|2|Defined|p124|Paleoproterozoic|Paleoproterozoic|See also p34. Type sections 3.2 miles southwest of Moolawatana Homestead and 4.4 miles south-southwest of Moolawatana Homestead, lat. 29degrees57'28"S long. 139degrees42'11"E to lat. 29degrees 57'45"S long. 139degrees 42'25" E and lat. 29degrees 58'32"S long. 139degrees 42'03"E  to lat. 29degrees58'44"S long. 139degrees42'08"E . Subsidiary type section: five miles northwest of Moolawatana Homestead, lat. 29degrees52'25"S long. 139degrees40'41"E to lat. 29degrees52'50"S long. 139degrees40'49"E.||||||24-NOV-22
25811|Brindana Schist|30807|6|Mentioned|p103|||Suggested map symbol||||||
25811|Brindana Schist|30920|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Prob.Lower Proterozoic||||||07-NOV-08
25811|Brindana Schist|34537|6|Mentioned|p35|||||||||
25811|Brindana Schist|41125|6|Mentioned|p50|||||||||
25811|Brindana Schist|43052|5|Briefly described|p96|||||||||
25811|Brindana Schist|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Mount Painter area.|1593 +/- 11 Ma.|||||
25811|Brindana Schist|67540|5|Briefly described|p33,35 Tb.2|||||Unit in Radium Creek Metamorphics.||Faulted against and/or intruded by Coulthard Suite. Overlies/faulted against Pepegoona Porphyry.||04-FEB-16
25811|Brindana Schist|68068|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Curnamona Province.||Unit in Radium Creek Metamorphics.|||Psammitic schist, muscovite-biotite schist, minor garnet-sericite schist, and calc-silicate rocks including epidote quartzite, hornfels, garnet rocks, skarns; multiple deformation fabrics common; lenses of cordierite-mica rock and para-amphibolite.|
25811|Brindana Schist|69023|4|Described|p16-17, p19-22, p53-55, p58, p187|Paleoproterozoic|Paleoproterozoic|Coats and Blissett (1971); modified by Teale (1993). A complex Formation of several meta-pelitic lithotypes, in Mount Babbage and Mount Painter Inliers, as keels, roof pendants and xenoliths within Mesozoic granites. No radiometric dating; age based on similarities with dated Willyama Supergroup in Olary region. Geochemistry detailed.||Unit in Radium Creek Metamorphics.||Is intruded by Terrapinna and Wattleowie Granites.|Dominantly muscovite and biotite schists which can contain porphyroblasts of garnet, andalusite and corundum; para-amphibolites and/or calc-silicates as lenses, bands and stringers; orthoamphibolites (meta-basalt); epidote-quartz rock.|
25811|Brindana Schist|69650|5|Briefly described|p8-9, p62, p64, p70, p74|||||Unit in Radium Creek Metamorphics.||Overlies Pepegoona Porphyry (tectonic contact, not conformably). Is intruded by Coulthard Suite. Is faulted against Box Bore Granite.||
25811|Brindana Schist|70384|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Two ?minor facies are mapped separately: para-amphibolite, calc-silicate; psammite, coarse-grained, micaceous, garnet-bearing (<2mm), well-preserved heavy mineral cross-bedding. Often exhibits multiple deformations: crenulations and kink bands. Metamorphic rims dated at 1556 +/- 10 Ma (ICPMS U-Pb zircon).|<1596 +/- 10 Ma (ICPMS U-Pb detrital zircon).|Radium Creek Group.|||Psammitic schist, muscovite and biotite schist, minor garnet sericite schist, and calc-silicate rocks including epidote quartzite, hornfels, garnet rocks and skarns. Lenses and discontinuous bands of cordierite-mica rock and para-amphibole.|
27039|Broadview Schist|22629|5|Briefly described|p152, figs2,4|Statherian|Statherian|Age: 1790Ma.||||||18-JAN-07
27039|Broadview Schist|23481|5|Briefly described|p19 Fig 1|||Geological Province: Gawler Craton.||||||
27039|Broadview Schist|23719|4|Described|p16|Paleoproterozoic|Paleoproterozoic|See also page 14 table 1. Overlain by McGregor Volcanics. Underlain by Myola Volcanics. Geol. Province: Gawler Craton.||||||07-NOV-08
27039|Broadview Schist|23805|5|Briefly described|p4 Fig. 1|Paleoproterozoic|Paleoproterozoic|Geological Province: Gawler Craton.||||||07-NOV-08
27039|Broadview Schist|24505|5|Briefly described|p5 Fig. 1|||Geological Province: Gawler Craton.||||||15-SEP-05
27039|Broadview Schist|37811|6|Mentioned|Fig.2|||||||||
27039|Broadview Schist|39349|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27039|Broadview Schist|39802|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27039|Broadview Schist|40448|5|Briefly described|p32|||||||||
27039|Broadview Schist|40644|5|Briefly described|p120,  p121, p129-130|Mesoproterozoic|Mesoproterozoic|Age: ca. 1470Ma; range of ca. 1600 to 1360Ma.||||||13-AUG-08
27039|Broadview Schist|41402|6|Mentioned|p35|||||||||
27039|Broadview Schist|41667|6|Mentioned|p6|||||||||
27039|Broadview Schist|41972|6|Mentioned|p365|||||||||
27039|Broadview Schist|42934|5|Briefly described|p520 Fig.1|||||||||
27039|Broadview Schist|43052|5|Briefly described|p62|||||||||
27039|Broadview Schist|43053|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Quartzite, schist, amphibolite.||||||07-NOV-08
27039|Broadview Schist|43258|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
27039|Broadview Schist|43298|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
27039|Broadview Schist|50605|6|Mentioned|p3.2, 11.1|||||||||
27039|Broadview Schist|60515|6|Mentioned|p116 Fig.1 |||||||||
27039|Broadview Schist|60953|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Schist, quartzite, amphibolite.||||||07-NOV-08
27039|Broadview Schist|60954|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Geological Province: Gawler Craton.||||||07-NOV-08
27039|Broadview Schist|61108|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|Schist, quartzite and amphibolite. Age: 1791 Ma.||||||07-NOV-08
27039|Broadview Schist|61262|5|Briefly described|p455 Fig. 11|Paleoproterozoic|Paleoproterozoic|Age: <1800Ma. Geological Province: eastern Gawler Craton.||||||07-NOV-08
27039|Broadview Schist|61307|5|Briefly described|p36 Fig. 17|Paleoproterozoic|Paleoproterozoic|Geological Province: Gawler Craton. See also p39 Fig. 19.||||||07-NOV-08
27039|Broadview Schist|61522|5|Briefly described|p5 Fig.1|||Geological Province: Gawler Craton.||||||
27039|Broadview Schist|64130|5|Briefly described|p1378 Fig.1 |Paleoproterozoic|Paleoproterozoic||~1790 Ma|||||
27039|Broadview Schist|64313|5|Briefly described|p450 Fig. 1|Paleoproterozoic|Paleoproterozoic|Age: <1800Ma. Geological province: Gawler Craton.||||||09-FEB-10
27039|Broadview Schist|64725|6|Mentioned|p58 Fig.2. |||Gawler Craton.||||||
27039|Broadview Schist|65221|5|Briefly described|p26|Palaeoproterozoic|Palaeoproterozoic|Volcano-sedimentary sequences overlying the Hutchison Group. Cleve Domain||||||
27039|Broadview Schist|65375|6|Mentioned|p13. |Paleoproterozoic|Paleoproterozoic||1791 Ma.|||||
27039|Broadview Schist|65376|6|Mentioned|p8 Fig.1.1. |Paleoproterozoic|Paleoproterozoic||||||Schist, quartzite, amphibolite and felsic volcanic rocks.|
27039|Broadview Schist|65390|5|Briefly described|p23 Fig.3|Statherian|Statherian|Spencer Domain, Gawler Craton. Overlies Myola Volcanics, underlies McGregor Volcanics. Age between 1790 - 1740 Ma inferred in Figure 3.||||||
27039|Broadview Schist|65915|5|Briefly described|p5|Statherian|Statherian|Sedimentary and volcanic rocks deposited between ~1790-1740 Ma east of Kalinjala Mylonite Zone.||||||
27039|Broadview Schist|65922|5|Briefly described|p13 Fig.4, p29 Fig. 6|Statherian|Statherian|Gawler Craton. Shown on Fig.6 as c.1790 Ma.||||||
27039|Broadview Schist|66302|6|Mentioned|p4 Fig.3, p28, p33, p57, p76 Fig.20, p88|Orosirian|Orosirian|Spencer Domain, Gawler Craton. |1795 +/- 5 Ma (Fraser and Neumann, 2010)||||Fine-grained slaty to phyllitic quartz-muscovite schist and fine-grained quartzite and amphibolite of the Broadview Schist.|
27039|Broadview Schist|66882|6|Mentioned|p102 Fig.2|Statherian|Statherian|Grouped with Myola Volcanics on figure.|1790 Ma|||||02-MAR-15
27039|Broadview Schist|67323|5|Briefly described|Eastern Australia Time-Space Plot; p31|||Eastern Gawler Craton.|1795 +/- 5 Ma (maximum depositional age).|||||
27039|Broadview Schist|67536|5|Briefly described|Map Legend|Statherian|Statherian|Gawler Craton.|ca. 1791 +/- 4 Ma||||Schist, quartzite, amphibolite.|
27039|Broadview Schist|67721|5|Briefly described|p36 Fig.6|Statherian|Statherian||c. 1790 Ma|||||
27039|Broadview Schist|68131|5|Briefly described|p2 Fig.1, p61|Paleoproterozoic|Paleoproterozoic|Mapped with Myola Volcanics as a single unit.|||||Included in a polygon of schist, quartzite, amphibolite and felsic volcanic rocks.|
27039|Broadview Schist|68158|5|Briefly described|p1-2, p4-8, p13-18, p20-21|||Sourced from SE Gawler Craton. Sm-Nd values. Deposition age and provenance discussed in detail.|1795 +/- 5 Ma (maximum depositional age).||||Light grey, fine-grained, mica and quartz sericite schist, feldspathic schist, minor fine-grained foliated metasandstone; white and pink, fine- to medium-grained foliated metasandstone; amphibolite lenses.|
27039|Broadview Schist|68208|6|Mentioned|p32 Fig.3, p33, p34 Fig.5, p35|Paleoproterozoic|Paleoproterozoic|Grouped with Myola Volcanics and described as terrestrial volcanics and sediments. Shows strong fabric from Kimban Orogeny.|C. 1790|||||
27039|Broadview Schist|69048|6|Mentioned|p3|||Eyre Peninsula / Yorke Peninsula.|c.1775-1750 Ma.|||||
27039|Broadview Schist|69649|6|Mentioned|p6 Fig.4,|||||||||
27039|Broadview Schist|69666|6|Mentioned|p27 Fig.3|Paleoproterozoic|Paleoproterozoic|||||||
27039|Broadview Schist|70334|5|Briefly described|p74|Statherian|Statherian|Geological province: Gawler Craton. |c. 1790 Ma|||Overlain by Moonabie Formation.||
27039|Broadview Schist|70659|4|Described|p4, p9-10, p14|Palaeoproterozoic|Palaeoproterozoic|Part of basement to the Spencer Domain. Kimban Orogeny (1730-1690 Ma) tectonic fabrics were folded by (~1620-1570 Ma) Kararan Orogeny.|<1795+/-5 Ma.|||Intruded by Tip Top Granite.|Fine-grained micaceous metasandstone with basaltic to gabbroic intrusions.|
27039|Broadview Schist|70721|5|Briefly described|p63-p66, p69-p70, p73-p75|Paleoproterozoic|Paleoproterozoic|Deposited in a shallow marine environment. Deformational fabrics are discussed.||||Intruded by the Tip Top Granite. Faulted against the Cooyerdoo Granite.|Sandstones and siltstones.|
27039|Broadview Schist|70816|6|Mentioned|p3-4|Paleoproterozoic|Paleoproterozoic|Gawler Ranges region. Underwent LT metamorphism during 1730-1690 Ma Kimban Orogeny.||||||
27039|Broadview Schist|70948|5|Briefly described|p974-975|Paleoproterozoic|Paleoproterozoic|Geological province: Gawler Craton.||||In faulted contact with Cooyerdoo Granite. Underwent LT metamorphism during 1730-1690 Ma Kimban Orogeny.||
27039|Broadview Schist|71037|5|Briefly described|p20-21, p21 Fig.1, p22-23 Fig.2, p24|Paleoproterozoic|Paleoproterozoic|Deposited in a marine shoreface environment. Maximum depositional age c. 1790 Ma (Szpunar and Fraser, 2010). See also p26, p27 Fig.6, p27. Deformtion event discussed.|c. 1795 - 1775 Ma|||Intruded by Wire Dam Dolerite, Tip Top Granite. Coeval with Myola Volanics. Shown as younger than Hutchison Group and older than Wertigo Granite.|Quartzite, laminated and fine-grained with interbedded shale. Deformed with a variably developed solid-state foliation.|
27039|Broadview Schist|71129|4|Described|p1,14,17-30,38,46,64,89|Statherian|Statherian|Geological Province: Spencer Domain, Gawler Craton. Nomenclature of Parker and Lemon (1982). Also referred to as Broadview Formation on p27. Thickness: original sedimentary package minimum estimate 13km, however uncertain due to absence of upper and lower contacts, and degree of deformation (see p21 for assumptions made); shows maximum thickness of 3km in seismic across the fault-bounded basin. Depositional environment: lower-middle marine shore face. Dominant unit in SW SIX MILE HILL, bounded to the east by N-striking Roopena Fault and south of Gawler Range Volcanics. Variably deformed package, deposited in a N-S trending fault-bounded basin; detritus from north and south. Lithologically subdivisible into two parts based on degree of strain; lower strain facies west of the Pankalla Fault, and higher strain facies between Pankalla and Roopena Faults. High strain facies is highly mylonitised in a 1.5km wide zone E-W and 16km long. Folded into NW-striking, upright, open structures with an axial planar foliation, coeval with and intruded by the c. 1775 Ma Tip Top Granite near Reilly Dam, and c. 1745 Ma Wortham Granite during Kimban Orogeny. Separated from Spearfelt Rhyodacite via Trevor Fault. Contains minor mafic sills of Wire Dam Suite. Previous geochronological analysis include c. 1809+\-12 Ma (MDA; quartzite; A. Reid, pers. comm. 2016), 1795 +\-5 Ma (MDA, quartzite, Szpunar and Fraser, 2010). Nd isotopic analysis of older ziron populations indicate possible detritus from Myola Volcanics, Cooyerdoo Granite, Coolanie Gneiss, Sleaford Complex and Bosanquet Formation or Donington Suite. Intruded by sills of the Wire Dam Dolerite (Wire Dam Suite). Faulted against the Moonabie and Wandearah formations. See also p104-105,142,155,177,180-181,183-184,188-194,196-199,203-207,225,227-228,231.|c. 1970 Ma (max dep)|||Overlain unconformably by Pandurra Formation, Gawler Range Volcanics, Umberatana Group. Underlain by Cooyerdoo Granite. Contemporaneous with Hutchison Group. Intruded by Tip Top and Wortham granites.|Pale brown to grey quartzites; medium- to coarse-grained, equigranular, well-sorted, with metamorphic textures, and showing strong foliation and evidence of recrystallisation in higher strain facies, with minor interbedded shales and siltstones.|13-NOV-19
27039|Broadview Schist|71130|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Maximum depositional age by Szpunar and Fraser (2010).|< c.1790 Ma.|||Is intruded by sills of Wire Dam Dolerite.|Quartzite, laminated and fine-grained with interbedded shale. Deformed with a variably developed solid-state foliation.|
27039|Broadview Schist|71131|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Maximum depositional age by Szpunar and Fraser (2010).|< c.1790 Ma.|||Is intruded by sills of Wire Dam Dolerite.|Quartzite, laminated and fine-grained with interbedded shale. Deformed with a variably developed solid-state foliation.|
27039|Broadview Schist|71235|5|Briefly described|p1, p3, p5-p6, p9|Palaeoproterozoic|Palaeoproterozoic|Deformed and metamorphosed to upper greenschist-amphibolite grade during the Kimban Orogeny.||||Unconformably overlain by the Corunna Conglomerate.||
27039|Broadview Schist|71317|6|Mentioned|p15-p16|Palaeoproterozoic|Palaeoproterozoic|Gawler Craton.||||||
27039|Broadview Schist|71341|6|Mentioned|p194, p196|||||||||
27039|Broadview Schist|71348|5|Briefly described|p201,208,212,214,217|Statherian|Statherian|Geological province: Gawler Craton. Coeval with Myola Volcanics eruption c. 1790 Ma. See p215 for summary of U-Pb geochronological data.||||||
27039|Broadview Schist|71413|5|Briefly described|p32, 33, 37|Statherian|Statherian|Geological province: Gawler Craton. |1791-1750 Ma|||Intruded by Samphire granite.||
27039|Broadview Schist|71414|6|Mentioned|p42 Fig 1, p43|Statherian|Statherian|Geological province: Gawler Craton.|~1790 Ma|||Intruded by Tip Top Granite, Wire Dam Dolerite.||
27039|Broadview Schist|71534|6|Mentioned|p296|Statherian|Statherian|Geological province: Gawler Craton.||||||
27039|Broadview Schist|71559|6|Mentioned|p15 Fig 1|Paleoproterozoic|Paleoproterozoic|Geological province: Gawler Craton.||||||
27039|Broadview Schist|71859|5|Briefly described|p3-p4, p6|Paleoproterozoic|Paleoproterozoic|Spencer Domain, southern Gawler Craton.||||||
27039|Broadview Schist|71862|6|Mentioned|p3, p8, p52-p53, p55||||c. 1790 Ma|||Intruded (inferred) by the Wortham Granite (Moola Suite) and the Peter Pan Supersuite.||12-APR-23
27039|Broadview Schist|72058|5|Briefly described|p171-p172|||Middleback Ranges, Gawler Craton. Associated with a period of intracontinental rifting.|~1791-1750 Ma|||||
27039|Broadview Schist|72089|6|Mentioned|p3|Palaeoproterozoic|Palaeoproterozoic|Gawler Craton.||||||
27039|Broadview Schist|72090|6|Mentioned|p8, p10, p14|Statherian|Orosirian|Gawler Craton.|c. 1865-1740 Ma|||||
27039|Broadview Schist|72237|6|Mentioned|p29|Paleoproterozoic|Paleoproterozoic|||||||
27039|Broadview Schist|72462|6|Mentioned|p3|Paleoproterozoic|Paleoproterozoic|Gawler Craton.||||||
27039|Broadview Schist|72463|6|Mentioned|p2, p4, p6|Paleoproterozoic|Paleoproterozoic|[Written as Broadview schist, p4, 6].||||Overlain by Corunna Conglomerate and Gawler Range Volcanics (unconformably).||
27039|Broadview Schist|72484|5|Briefly described|p3, 22|||Eyre Peninsula, Gawler Craton. Contains zircons inherited from the 2823 +/- 37 Ma protolith of Coolanie Gneiss.|~1791-1750 Ma.|||||
27039|Broadview Schist|73026|5|Briefly described|p6-7, p9|Paleoproterozoic|Paleoproterozoic|Northern Eyre Peninsula/Yorke Peninsula.|c. 1750 Ma|||Underlies the Wallaroo Group.||
27039|Broadview Schist|73027|5|Briefly described|p6-p7, p9|Palaeoproterozoic|Palaeoproterozoic|Eastern Eyre Peninsula/Yorke Peninsula. Associated with the Myola Volcanics.|c. 1790 Ma|||||
27039|Broadview Schist|73030|6|Mentioned|p2148-2149|Statherian|Statherian|Gawler Craton.||||||
27039|Broadview Schist|73103|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|||||Is intruded by sills of Wire Dam Dolerite.|Schist, thin-bedded, fine-grained, slaty to phyllitic fine-grained quartzite and amphibolite.|
27039|Broadview Schist|73110|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|||||Is intruded by Wire Dam Dolerite (as sills).|Schist, thin-bedded, fine-grained, slaty to phyllitic fine-grained quartzite and amphibolite.|
27039|Broadview Schist|73130|6|Mentioned|[poster] Fig.1|Paleoproterozoic|Paleoproterozoic|||||||28-OCT-22
27039|Broadview Schist|73162|6|Mentioned|p449, p450 Fig.2, p451, p452 Fig.3|Paleoproterozoic|Paleoproterozoic||||||Includes hematite and silica alteration at the Spencer Prospect, west of the Roopena Basin.|
27039|Broadview Schist|73234|6|Mentioned|p4, p19|Statherian|Statherian[?]|[Among the] oldest rocks exposed on Six Mile Hill. Deposited in volcano-sedimentary basins that developed on older Archean to Paleoproterozoic crystalline basement of the Gawler Craton. Age also written as deposited at c. 1795-1775 Ma.|c. 1790 Ma|||||
27039|Broadview Schist|73235|6|Mentioned|p53, p58, p61, p63|||Gawler Craton. Spencer region. Hosts mineralisation in the Southern Gawler Range Volcanics mineral field of the Kararan (Gawler Range Volcanics) gold mineral system and in the Wudinna and Olympic mineral field of the Kararan (Hiltaba Suite) gold mineral system. May host gold mineralisation in the Middleback mineral field of the Kimban gold mineral system but no discoveries are yet known.||||||
27039|Broadview Schist|73493|6|Mentioned|p716 Fig.3|||Gawler Craton.||||||
27039|Broadview Schist|73525|5|Briefly described|p19 Fig.13|Statherian|Statherian|Spencer Domain.|1795+/-5 Ma maximum depositional age||||Clastics.|
38065|Bronze Whaler Supersequence|24336|5|Briefly described|p99 Fig.3|||Correlated to the Borda Formation.||||||
38065|Bronze Whaler Supersequence|61544|6|Mentioned|p367 Fig.3. |Albian|Valanginian|Ceduna Sub-basin. Post-rift slow thermal subsidence.||||Overlies Southern Right Supersequence. Is overlain by Blue Whale Supersequence.||
38065|Bronze Whaler Supersequence|66578|6|Mentioned|p1007 Fig.3.|Early Cretaceous|Early Cretaceous|Ceduna Sub-Basin, Bight Basin.||||Overlies Southern Right Supersequence. Is overlain by Blue Whale Supersequence.||
38065|Bronze Whaler Supersequence|69297|5|Briefly described|p14 fig 2.4, p23, p25 fig 2.9|Albian|Valanginian|Eyre, Ceduna and Duntroon Sub-basins. Deposited in lacustrine and fluvial environments. Displays good oil potential in the fine-grained lacustrine facies of this sequence. Excellent fault seal capacity for hydrocarbons.  Contains potential source rocks within lacustrine shales and coaly deposits. See also p26 fig 2.11, p27, p28, p37, p42, p45 fig 2.17, p58, p60, p61.||||Overlies the Southern Right Supersequence. Overlain by the Blue Whale Supersequence.|Interbedded claystone, siltstone, snadstone and coal.|
38065|Bronze Whaler Supersequence|70067|5|Briefly described|Ceduna: Fig.2; p2. Regional: Fig.2|Albian|Valanginian|Bight Basin. Comprises all but the topmost part of Borda Formation. Potential reservoir.||||Overlies Southern Right Supersequence. Is overlain by Blue Whale Supersequence.||
38065|Bronze Whaler Supersequence|71618|6|Mentioned|p131|Albian|Valanginian|Of Bight Basin. Fluvial-lacustrine sedimentary succession.|140-100 Ma|||||
31514|Bryant Creek Formation|23179|6|Mentioned|p32, Fig.2||Middle Miocene|Parent: Morgan Group, gp:Murray Basin.||||||
31514|Bryant Creek Formation|23226|2|Defined|p900||Balcombian|Was informally known as Upper Morgan Limestone. Age: Balcombian by fossil assemblage of foraminifers and stratigraphic position. Of Morgan Group.||||||
31514|Bryant Creek Formation|23768|5|Briefly described|p34|||Recognised by Lukasik and James (1993) as a distinct unit of Morgan Limestone (now recognised as a group). Geological Province: Murray Basin.||||||30-MAR-05
31514|Bryant Creek Formation|24558|4|Described|p655 Fig. 3|Middle Miocene|Middle Miocene|Low energy carbonate ramp sediments with with abundant bryozoans. Conformably overlies Cadell Formation; conformably overlain by Pata Formation.||||||12-APR-05
31514|Bryant Creek Formation|63460|5|Briefly described|p839 Fig. 2b|Middle Miocene|Middle Miocene|Geological province: Murray Basin. Limestone-rich unit.||||||
31514|Bryant Creek Formation|64237|5|Briefly described|p19 Fig.2b|Middle Miocene|Middle Miocene|Unit recognised by Lukasik and James (1998) within their Morgan Group (Murray Supergroup); underlying Pata Formation, overlying Cadell Formation. Name has been retained but is now within the Morgan Subgroup, following the reinstating of the Murray Group||||||15-JUL-08
31514|Bryant Creek Formation|72445|6|Mentioned|App.6 p2 Fig.1.|Middle Miocene|Middle Miocene|Of Lukasik and James (1998).||Murray Supergroup||Overlies Cadell Formation and underlies Pata Formation?|Includes limestone.|
30504|Buccleuch Formation|10010|5|Briefly described|p12 Fig. 3|Late Eocene|Middle Eocene|Geological Province: Murray Basin.||||||13-AUG-07
30504|Buccleuch Formation|22587|6|Mentioned|p79 Fig.7|Late Eocene|Late Eocene|||||||
30504|Buccleuch Formation|22773|5|Briefly described|p351,Fig24.8p352|Eocene|Late Eocene|||||||
30504|Buccleuch Formation|22857|5|Briefly described|p351, p352 Fig.24.8|Late Eocene|Late Eocene|Marine deposits. Geological Province: Murray Basin. Equivalents mentioned on p352 Fig.24.8. See also p353 Fig. 24.9.||||||
30504|Buccleuch Formation|43195|5|Briefly described|Map Legend|Early Oligocene|Late Eocene|||||||
30504|Buccleuch Formation|44133|5|Briefly described|p158, 152 Fig. 10.2|Late Oligocene|Late Eocene|Formerly Buccleuch Beds, Buccleuch Group. Geological Province: Murray Basin.  ||||||
30504|Buccleuch Formation|60785|5|Briefly described|p184 Fig.1, p195.  |Rupelian|Rupelian|South Australia. Has yielded a fossil cetacean heterodont tooth.|||||Green and slightly glauconitic fine-grained limestone.|
30504|Buccleuch Formation|63887|5|Briefly described|p20, p21 Fig. 1|Late Eocene|Late Eocene|Of Renmark Group[?]. Marnie incursion indicated by deposition of fossilerous clay and marl.||||||03-DEC-13
30504|Buccleuch Formation|67462|5|Briefly described|Map legend.|Oligocene|Oligocene|Murray Basin.||||||
30504|Buccleuch Formation|68715|6|Mentioned|p31 Fig.5|Oligocene|Eocene|Murray Basin. Late Eocene to Late Oligocene age.||||||
30504|Buccleuch Formation|73188|6|Mentioned|p320|Oligocene|Oligocene|Murray Basin.|||||Limestone, marl, clay.|
30504|Buccleuch Formation|73228|4|Described|p50, p54-57, p60|Late Eocene|Late Eocene|Murray Basin, northern SA. Resulted from a minor marine incursion. Grades laterally into the marginal marine upper Olney Formation.||Renmark Group|||Bryozoal and glauconitic limestones, bryozoal clayey sand, and black pyritic/ferruginous clay.|
30504|Buccleuch Formation|73229|6|Mentioned|p67|Early Oligocene|Late Paleocene|Murray Basin.||Renmark Group||||
75515|Bumbumbie Suite|70405|5|Briefly described|p36|Paleoproterozoic|Paleoproterozoic|None represented in study area.|1710 Ma - 1720 Ma|Kalabity Supersuite|Includes Montstephen Subsuite, Tietz Subsuite,||Mafic igneous rocks.|
25818|Bunburn Dacite|24474|3|Fully described|p40|||Of the Glyde Hill Volcanic Complex.  Ranges from basaltic andesite to rhyodacite.  Overlain by Baldry Rhyolite; conformably overlies Nuckulla Basalt.  Max. thickness: 100m.  Geological Province: Gawler Craton.||||||
25818|Bunburn Dacite|30984|2|Defined|p13|Proterozoic|Proterozoic|||||||
25818|Bunburn Dacite|41974|6|Mentioned|p411|||||||||
25818|Bunburn Dacite|42546|5|Briefly described|Map legend|Mesoproterozoic||||||||
25818|Bunburn Dacite|42721|5|Briefly described|map legend|Carpentarian||||||||
25818|Bunburn Dacite|42722|5|Briefly described|map legend|Carpentarian|Carpentarian|Of the Glyde Hill Volcanic Complex.  At base, dark purplish-grey, pale grey and purplish lapilli tuff and flowbanded porhpyritic rhyodacitic welded tuff; overlain by dark greenish-grey dacite passing up into reddich-brown rhyodacite. Overlain by Nuckulla||||||07-APR-05
25818|Bunburn Dacite|42736|5|Briefly described|map legend|Mesoproterozoic||||||||
25818|Bunburn Dacite|43052|5|Briefly described|p111|||of Glyde Hill Volcanic Complex||||||
25818|Bunburn Dacite|43071|5|Briefly described|p14,Table 2|||of Gawler Range Volcanics||||||
25818|Bunburn Dacite|43094|4|Described|table 4.|||of Glyde Hill Volcanic Complex||||||
25818|Bunburn Dacite|67909|6|Mentioned|p126-128|Mesoproterozoic|Mesoproterozoic|Lake Everard area. Volcanic textures and emplacement mechanism tabulated.||Glyde Hill Volcanic Complex.||||
25818|Bunburn Dacite|69649|5|Briefly described|p21-23|Mesoproterozoic|Mesoproterozoic|Giles (1977). A laterally extensive unit. 30-100m thick.||Unit in Glyde Hill Volcanic Complex.||Is overlain by Baldry Rhyolite and (conformably) by Nuckulla Basalt.|Phenocryst-poor, basaltic andesite to rhyodacite; rare K-feldspar phenocrysts, localised layering; contains prominent perlite up to 50cm diameter.|24-FEB-15
25818|Bunburn Dacite|70659|5|Briefly described|p6-8|Mesoproterozoic|Mesoproterozoic|Represents a single volcanic flow.||Glyde Hill Volcanic Complex.||Is overlain conformably by Nuckulla Basalt.|Dacite.|
25818|Bunburn Dacite|70816|5|Briefly described|p5|||Lake Everard area, Gawler Ranges.||Unit of Glyde Hill Volcanic Complex.||Overlain by Baldry Rhyolite. Underlain by Waurea Pyroclastics.||07-JUL-20
25818|Bunburn Dacite|72090|6|Mentioned|p12|||Gawler Craton.||Glyde Hill Volcanic Complex||||
80744|Bunburra Suite|72242|5|Briefly described|p27,29-31|Calymmian|Calymmian|Geological province: Coompana Province. Represents a newly reported magmatic event, based on juvenile isotopic character and primitive geochemical signatures (Dutch 2018; Jagodzinski and Bodorkos 2018). Interpreted to be derived from a subduction-enriched lithospheric mantle source (Dutch, 2018).|c. 1527 Ma||||Migmatitic orthogneisses.|29-NOV-22
80744|Bunburra Suite|72344|5|Briefly described|p3, p7, p9, p63|Calymmian|Calymmian|Coompana Province. Intersected in drillhole CDP004. Metamorphosed at 1197 +/- 12 Ma (SHRIMP; this volume). Petrography, SHRIMP analyses and geochemistry are discussed for a sample.|1526+/-5 Ma SHRIMP magmatic age.|Undawidgi Supersuite|||Massive, equigranular, medium-grained mesocratic, hornblende-biotite dioritic gneiss.|04-SEP-19
80744|Bunburra Suite|72934|6|Mentioned|p4, p11, App.A|||Associated with, but slightly predates Undawidgi Supersuite magmatism. Yielded a U-Pb SIMS zircon magmatic crystallisation age of 1526 +/- 6 Ma and a metamorphic age of 1199 +/- 17 Ma.||||||
80744|Bunburra Suite|72947|2|Defined|p7-9, p11-14, p18, p21|Calymmian|Calymmian|Coompana Province, eastern. Named after Bunburra Rockhole. No known surface exposures. Type locality [only locality]: CDP004 (drillhole 299058, interval 491.39-547.18 m). Age listed is of the protolith. Age of high-grade metamorphism [and partial melting]: 1197 +/- 12 Ma (SHRIMP U-Pb). Represents a newly recognised magmatic event in the region (Dutch, 2018; Jagodzinski et al., 2019). Juvenile isotopic character and primitive geochemical signatures, indicating the Bunburra Suite was derived from a subduction-enriched lithospheric mantle source in a subduction setting (Dutch, 2018). Compositionally and temporally distinct from the nearby Undawidgi Supersuite; thus, not currently assigned to a supersuite. [Partly?] underwent magmatic-state deformation and flow. Occurs in a wedge between the Border and Bunburra shear zones. Sheared contact with the Toolgana Supersuite to the northwest. Partly sheared contact with the Koonalda Suite to the southeast.|1526 +/- 5 Ma (SHRIMP U-Pb)|||Intruded by Merdayerrah Shoshonite and Giants Head Suite. Partly intruded by Koonalda Suite. Sheared contact with Toolgana Supersuite.|Dioritic to quartz-dioritic migmatitic orthogneisses. Fine to very coarse grained, dominantly plagioclase and hornblende, with quartz, biotite and K-feldspar as minor phases. Schlieren or schollen diatexites.|
80744|Bunburra Suite|72949|6|Mentioned|p40|Calymmian|Calymmian|Coompana Province. Represents episodic magmatism with subduction-related, arc-type geochemistry.|c. 1.53 Ga|||||
80744|Bunburra Suite|73084|5|Briefly described|p124, p129, p137, p142|Calymmian|Calymmian|Coompana Province. Isotopically juvenile. Formed in a subduction setting. Slightly older than the Undawidgi Supersuite. Compositionally similar to mafic members of the older Toolgana Supersuite. May represent westward-migrating arcs.|1526 +/- 5 Ma|||Intruded by Merdayerrah Shoshonite.|Dominated by migmatitic, hornblende-biotite diorite gneiss.|
80744|Bunburra Suite|73091|5|Briefly described|Mapsheet|Calymmian|Calymmian||c. 1527 Ma||||Migmatitic orthogneiss.|30-NOV-21
80744|Bunburra Suite|73224|5|Briefly described|p42-44|Calymmian|Calymmian|Coompana Province, northeast-trending corridor. Juvenile isotopic character and primitive geochemical signatures. Derived from a subduction-enriched lithospheric mantle source. Metamorphism and partial melting at 1197 +/- 12 Ma.|1526 +/- 5 Ma||||Migmatitic orthogneisses.|
80744|Bunburra Suite|73225|5|Briefly described|p2, 4, p22 Fig.10|||Coompana Province. East of the Mulyawarra Shear Zone. Unassigned.|1526 Ma.|||||
80744|Bunburra Suite|73234|6|Mentioned|p19|Calymmian|Calymmian|Coompana Province. Age from Wise, Pawley and Dutch (2018).|c. 1525 Ma|||||
80744|Bunburra Suite|73641|5|Briefly described|p2|||Derived from a subduction-modified enriched lithospheric mantle.|1520 Ma|||Is intruded by Giants Head Suite.|Gneisses; diorite.|
25686|Bungadillina Monzonite|23054|5|Briefly described|p15-7,21,33||Late Cambrian|Max Age: 497.5 (+/-) 10.4 Ma (Fanning, in prep.).||||||
25686|Bungadillina Monzonite|24506|5|Briefly described|p16|Late Cambrian|Late Cambrian|Intrusive plutons.  Age: 497.5+/-10.4Ma.||||||
25686|Bungadillina Monzonite|36733|2|Defined|p68|Ordovician|Ordovician|See also P52.||||||
25686|Bungadillina Monzonite|42222|6|Mentioned|p26|||||||||
25686|Bungadillina Monzonite|42274|5|Briefly described|p450|||||||||
25686|Bungadillina Monzonite|43052|5|Briefly described|Fig.4.33|||||||||
25686|Bungadillina Monzonite|44133|5|Briefly described|p54,56 Table 7.3|Cambrian|Cambrian|Of the Peake and Denison Inliers. Quartz monzonite to syenogabbro. A-Type. Age: 521 +/- 35Ma, 527 +/- 27Ma.||||||
25686|Bungadillina Monzonite|44289|5|Briefly described|Map Legend|Ordovician|Late Cambrian|||||||
25686|Bungadillina Monzonite|67536|5|Briefly described|Map Legend|Guzhangian|Ediacaran|Kanmantoo Province; basement to Murray Basin.|ca. 527 +/- 27 Ma||||Pre/syn-Delamerian felsic intrusive rocks.|
25686|Bungadillina Monzonite|70938|5|Briefly described|p807-809, p812, p814-815|Ordovician|Ordovician|Davenport Range. Associated with the Delamerian Orogeny. Other ages are also given.|497.5 +/- 10 Ma; Rogers and Freeman (1994).||||A series of monzonites, syenites, gabbros and dykes.|13-DEC-19
25686|Bungadillina Monzonite|73118|6|Mentioned|p73|||Probably related to early Delamerian Orogeny.|527 +/- 27 Ma (Fanning, 1987).|||||
25819|Bungaree Quartzite|22869|6|Mentioned|P37, Table2|||||||||
25819|Bungaree Quartzite|22889|4|Described|p31|Adelaidean|Adelaidean|Parent - Emeroo Subgroup.  The original definition of the Bungaree Quartzite found in the Mid-North and Nackara Arc,  is revised.||||||
25819|Bungaree Quartzite|24175|6|Mentioned|p11|||Of the BURRA region.||||||
25819|Bungaree Quartzite|35328|2|Defined|p11|Adelaidean|Adelaidean|||||||
25819|Bungaree Quartzite|36244|6|Mentioned|p2|||Defined by Forbes 1977.||||||
25819|Bungaree Quartzite|36733|6|Mentioned|Table 5|||See also P23.||||||
25819|Bungaree Quartzite|37461|6|Mentioned|Table 5.I|||||||||
25819|Bungaree Quartzite|37854|6|Mentioned|p15|||||||||
25819|Bungaree Quartzite|38157|6|Mentioned|Table III|||||||||
25819|Bungaree Quartzite|38926|6|Mentioned|p31|||||||||
25819|Bungaree Quartzite|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Torrensian||||||
25819|Bungaree Quartzite|40294|6|Mentioned|p9|||See also Table 1||||||
25819|Bungaree Quartzite|41404|3|Fully described|p84|||||||||
25819|Bungaree Quartzite|42222|6|Mentioned|p13|||||||||
25819|Bungaree Quartzite|43052|5|Briefly described|p177,Table 6.2|||Emeroo Subgroup||||||
25819|Bungaree Quartzite|64796|5|Briefly described|p191 Fig.9, p192|Neoproterozoic|Neoproterozoic|Lobate deltaic sand body.||||Overlies Benbournie Dolomite. Is overlain by Skillogalee Dolomite.||
25819|Bungaree Quartzite|70405|6|Mentioned|p51 table 4|Neoproterozoic|Neoproterozoic|||Emeroo Subgroup|||Siliciclastic metasediments.|
25819|Bungaree Quartzite|70819|6|Mentioned|p13, 19|Neoproterozoic|Neoproterozoic|Clare Valley.||Emeroo Subgroup.||||
25819|Bungaree Quartzite|73110|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic||||||Sandstone, fine- to coarse-grained, feldspathic, quartzitic, to arkosic, ripple marks, cross-bedding, lenticular, minor pale grey to greenish siltstone, minor pale grey dolomite.|
23441|Bungarider Subgroup|22889|2|Defined|p35|Adelaidean|Adelaidean|Former name Bungarider Subgroup (by Murrell,1977) lapsed from reservation. The term Bungarider Subgroup is resurrected and its constituent formations extended, see p31 and p35 for details of new Definition.||||||14-MAY-07
23441|Bungarider Subgroup|37461|6|Mentioned|Fig.5.13|||||||||
23441|Bungarider Subgroup|38108|6|Mentioned|Table 1|||||||||
23441|Bungarider Subgroup|60718|5|Briefly described|p49 Fig. 2, p52|Adelaidean|Adelaidean|Geological Province: Adelaide Geosyncline.||Of Burra Group.|Includes Myrtle Springs Formation.|||15-APR-11
23441|Bungarider Subgroup|61238|5|Briefly described|p44 Fig. 1|Neoproterozoic|Neoproterozoic|Of the Burra Group.||||||
23441|Bungarider Subgroup|62592|5|Briefly described|p50 Table 5.1, p57.|Torrensian|Torrensian|Adelaide Geosyncline.||Unit in Burra Group.||Overlies Mundallio Subgroup. Is overlain by Belair Subgroup.|Siltstone, sandstone, deep-water dolomite.|
23441|Bungarider Subgroup|62724|5|Briefly described|p17 Fig. 4|Torrensian|Torrensian|Of the Burra Group. Overlies Skillogalee Dolomite.||||||07-FEB-11
23441|Bungarider Subgroup|66522|5|Briefly described|p20 Fig.2, p23.|Neoproterozoic|Neoproterozoic|||Unit in Burra Group.|Includes Woolshed Flat Shale, Undalya Quartzite and Saddleworth Formation.|Rests on an erosive surface cut to varying depths into Skillogalee Dolomite.|Grey-green, laminated siltstone.|
23441|Bungarider Subgroup|66884|5|Briefly described|p36, p39 Fig.2, p41 Fig.3|||||Burra Group|Myrtle Springs Formation|||
23441|Bungarider Subgroup|67870|5|Briefly described|p9|Neoproterozoic|Neoproterozoic|Adelaide Rift System.||Burra Group.||||
23441|Bungarider Subgroup|69019|6|Mentioned|p41.|Neoproterozoic|Neoproterozoic||||Includes Myrtle Springs Formation.|||
23441|Bungarider Subgroup|70384|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Adelaide Geosyncline.  Age shown more specifically as Torrensian [Cryogenian].||Burra Group.|Includes Myrtle Springs Formation.|Overlies Mundallio Subgroup. Is overlain unconformably by Yudnamutana Subgroup (Umberatana Group).||18-JAN-19
23441|Bungarider Subgroup|70405|6|Mentioned|p50, p51 table 4|Neoproterozoic|Neoproterozoic||||Includes Saddleworth Formation, Undalya Quartzite, Woolshed Flat Shale|||
23441|Bungarider Subgroup|70819|6|Mentioned|p11, 13-14, 18|Neoproterozoic|Neoproterozoic|Clare Valley. Marine deposits.||Burra Group.|Woolshed Flat Shale, Saddleworth Formation, Undalya Quartzite, Watervale Sandstone.|Disconformably overlies Mundallio Subgroup. Is overlain unconformably by Belair Subgroup.||
23441|Bungarider Subgroup|73188|6|Mentioned|p316|Neoproterozoic|Neoproterozoic|Mount Lofty Ranges.||Burra Group|Saddleworth Formation, Beaumont Dolomite Member, Stonyfell Quartzite, Woolshed Flat Shale|||
23441|Bungarider Subgroup|74367|5|Briefly described|p3, p7 Fig.6, p8|Tonian|Tonian|||Burra Group|Woolshed Creek Shale, Undalya Quartzite, Saddleworth Formation|||
28415|Bunkers Sandstone|22766|5|Briefly described|Fig.2 p561, p561|Early Cambrian|Early Cambrian|||||||
28415|Bunkers Sandstone|23818|4|Described|p87 Fig.33, p91|Cambrian|Cambrian|Of the Hawker Group. Max. thickness: 600 ft.||||||
28415|Bunkers Sandstone|23981|5|Briefly described|p8-9 Fig.4, p10 Fig. 5|Early Cambrian|Early Cambrian|Age is Botomian. Geological Province: Arrowie Basin. See also p52 Fig. 20.||||||12-JUL-06
28415|Bunkers Sandstone|24072|5|Briefly described|p369 Fig.1|Cambrian|Cambrian|Geological Province: Great Artesian Basin.||||||
28415|Bunkers Sandstone|24465|5|Briefly described|p345 Fig.2|Early Cambrian|Early Cambrian|Of the Hawker Group.  Geological Province: Arrowie Basin.||||||19-JAN-05
28415|Bunkers Sandstone|29929|6|Mentioned|Fig.1|||||||||
28415|Bunkers Sandstone|30051|6|Mentioned|p20|||||||||
28415|Bunkers Sandstone|30801|6|Mentioned|p5|||Hawker Group. Table P5-6||||||
28415|Bunkers Sandstone|30802|5|Briefly described|p11|||Cambrian age||||||
28415|Bunkers Sandstone|30807|6|Mentioned|p102|||Suggested map symbol||||||
28415|Bunkers Sandstone|31706|6|Mentioned|p633|||Cambrian correlation chart||||||
28415|Bunkers Sandstone|33474|6|Mentioned|Fig.3|||||||||
28415|Bunkers Sandstone|33932|4|Described|p17|||||||||
28415|Bunkers Sandstone|33934|6|Mentioned|Fig.2|||L.Camb.||||||
28415|Bunkers Sandstone|34269|6|Mentioned|Table 1|||Cambrian||||||
28415|Bunkers Sandstone|34612|4|Described|p91|||Fig.33||||||
28415|Bunkers Sandstone|35075|6|Mentioned|p77|||||||||
28415|Bunkers Sandstone|35255|6|Mentioned|Fig.8|||||||||
28415|Bunkers Sandstone|35395|6|Mentioned|p105|||||||||
28415|Bunkers Sandstone|36198|6|Mentioned|Fig.I.2|||||||||
28415|Bunkers Sandstone|36495|6|Mentioned|p117|||||||||
28415|Bunkers Sandstone|36525|6|Mentioned|Fig.4|||See also Fig.5.||||||
28415|Bunkers Sandstone|38068|6|Mentioned|p69|||||||||
28415|Bunkers Sandstone|40431|6|Mentioned|p12|||||||||
28415|Bunkers Sandstone|40672|6|Mentioned|Fig.2|||||||||
28415|Bunkers Sandstone|40831|6|Mentioned|Fig.2|||||||||
28415|Bunkers Sandstone|40852|6|Mentioned|Fig.3.7|||||||||
28415|Bunkers Sandstone|40856|6|Mentioned|Fig.23.6|||||||||
28415|Bunkers Sandstone|41457|6|Mentioned|Fig.1|||||||||
28415|Bunkers Sandstone|41526|6|Mentioned|p61|||||||||
28415|Bunkers Sandstone|41996|4|Described|p7|||see also Fig.2 P6||||||
28415|Bunkers Sandstone|42011|6|Mentioned|Fig.3 P458|||||||||
28415|Bunkers Sandstone|42192|6|Mentioned|p10|||||||||
28415|Bunkers Sandstone|42213|4|Described|p474|||See also Fig.2||||||
28415|Bunkers Sandstone|42222|6|Mentioned|Table 1 P5|||||||||
28415|Bunkers Sandstone|42225|6|Mentioned|Fig.4 P224|||||||||
28415|Bunkers Sandstone|42226|6|Mentioned|p231|||||||||
28415|Bunkers Sandstone|42233|6|Mentioned|Fig.1 P248|||||||||
28415|Bunkers Sandstone|42247|6|Mentioned|p9|||||||||
28415|Bunkers Sandstone|42272|6|Mentioned|p414|||||||||
28415|Bunkers Sandstone|42440|6|Mentioned|Fig.2 P602|||||||||
28415|Bunkers Sandstone|42458|5|Briefly described|Fig.2 P699|||||||||
28415|Bunkers Sandstone|43845|6|Mentioned|Fig4 p44|||||||||12-JUL-16
28415|Bunkers Sandstone|44133|5|Briefly described|p4 Fig. 7.2, 24|Early Cambrian|Early Cambrian|Geological Province: Arrowie Basin. Maximum Thickness: 200m. ||||||
28415|Bunkers Sandstone|60418|5|Briefly described|p135|Early Cambrian|Early Cambrian|Of Hawker Group. Geological Province: Arrowie Basin of Adelaide Geosyncline.||||||
28415|Bunkers Sandstone|60889|4|Described|p245 Fig.2, p249|Early Cambrian|Early Cambrian|Thickness: 300 m. Lowstand. Comprises mainly cross-bedded quartz sandstone in Bunkers Graben, but in Donkey Bore Syncline (north of Wirrealpa Hill Hinge) comprises deeper-water basin-floor fan deposits. Arrowie Basin.||Hawker Group||Disconformably overlies middle Wilkawillina Limestone. Is overlain by Oraparinna Shale.|Comprises mainly cross-bedded quartz sandstone.|
28415|Bunkers Sandstone|60959|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of the Hawker Group. Thin basal sequence of flat to ripple laminated, silty fine-grained quartz sandstone, overlain by medium grained quartz sandstone.||||||
28415|Bunkers Sandstone|60990|5|Briefly described|p83 Fig.2|Botoman|Botoman|Flinders Ranges.||Hawker Group.||||
28415|Bunkers Sandstone|62784|5|Briefly described|p8 Fig.1, p10 Fig. 3|Cambrian|Cambrian|Arrowie Basin. Unit in Hawker Group disconformably overlying Mernmerna Formation. Underlies Oraparinna Shale.||||||
28415|Bunkers Sandstone|63447|5|Briefly described|p962,p963 Fig.2 |Early Cambrian|Early Cambrian|||Hawker Group||Lateral equivalent to Mernmerna Formation.|Calcareous sandstone and sandy limestone.|
28415|Bunkers Sandstone|63569|6|Mentioned|p117, p119-120|Cambrian|Cambrian|Arrowie Basin.||Unit in Hawker Group.||Disconformably overlies Mernmerna Formation. Is overlain conformably by Oraparinna Shale.||
28415|Bunkers Sandstone|64829|5|Briefly described|p1084-5 Figs.1,  2|Early Cambrian|Early Cambrian|||||||07-FEB-11
28415|Bunkers Sandstone|65313|6|Mentioned|p576 Fig. 5,  p578 Fig. 6|Early Cambrian|Early Cambrian|||Of Hawker Group.||||26-MAR-12
28415|Bunkers Sandstone|65375|5|Briefly described|p33.|Early Cambrian|Early Cambrian|||Unit in Hawker Group.||Overlies Mernmerna Formation. Is overlain by Oraparinna Shale.||
28415|Bunkers Sandstone|65625|5|Briefly described|p103 Fig.2|Early Cambrian|Early Cambrian|Lake Frome area.||||Overlies Parara Limestone. Underlies Oraparinna Shale.||18-FEB-11
28415|Bunkers Sandstone|65686|5|Briefly described|p412,  p409 Fig 2|Early Cambrian|Early Cambrian|Arrowie Basin. 300m thick.||||Underlies the Oraparinna Shale.||07-MAY-12
28415|Bunkers Sandstone|65892|5|Briefly described|p7 Fig.3, p9 Fig.4, p10, p44. |Early Cambrian|Early Cambrian|Arrowie Basin. 300m thick.||Unit in Hawker Group.||Overlies Mernmerna Formation. Is overlain by Oraparinna Shale.|Cross-bedded quartz sandstone; also deeper water basin-floor fan deposits.|
28415|Bunkers Sandstone|65925|6|Mentioned|p14 Fig.2.2.|Early Cambrian|Early Cambrian|||||||
28415|Bunkers Sandstone|68735|5|Briefly described|p233 Fig.2, p234, p235 Fig.3|Early Cambrian|Early Cambrian|Arrowie Basin. < 300 m thick in the Bunkers Graben, but elsewhere it is thin or missing.||Of the Hawker Group.|||Cross-bedded sandstone.|
28415|Bunkers Sandstone|68993|6|Mentioned|p544 Fig.1|Early Cambrian|Early Cambrian|Arrowie Basin.||Of the Hawker Group.||||
28415|Bunkers Sandstone|69570|6|Mentioned|p421 fig 1|Cambrian|Cambrian|Arrowie Syncline, Flinder Ranges.||||||
28415|Bunkers Sandstone|70833|6|Mentioned|p200-201|Series 2|Series 2|||Unit of Hawker Group.||||
28415|Bunkers Sandstone|70835|6|Mentioned|p335-337|Cambrian|Cambrian|Arrowie Basin, Flinders Ranges.||Hawker Group.||Overlies Mernmerna Formation. Is overlain by Oraparinna Shale.||
28415|Bunkers Sandstone|71102|5|Briefly described|p242,244-246,251,263,267|Series 2|Series 2|Of Arrowie Basin. Variably developed arkosic unit in the central and eastern Arrowie Basin. Intersected sections: DBS (Donkey Bore Syncline), MMF (Bunkers Range, Central Flinders Ranges), 10MS (10 Mile South, Bunkers Graben).|||||Debris-flow quartz sandstone with minor feldspar, crossbeds.|
28415|Bunkers Sandstone|72449|5|Briefly described|p2 Map Legend|Cambrian|Cambrian|||||Overlies Mernmerna Formation and underlies Oraparinna Shale.|Silty fine-grained sandstone with cross-bedding and ripple marks.|
28415|Bunkers Sandstone|73255|6|Mentioned|p534 Fig.2|early Cambrian|early Cambrian|||||Overlies the Wilkawillina Limestone, underlies the Oraparinna Shale||
28299|Bunyeroo Formation|7931|5|Briefly described|p98, p99 Fig. 2|Ediacaran|Ediacaran|Of the Wilpena Group. The lower part of this unit is an important regional chronostratigraphic marker - the Acraman impact horizon. Deep-water mudstones.||||||07-FEB-11
28299|Bunyeroo Formation|22646|6|Mentioned|Fig 4 on p 102|Neoproterozoic|Neoproterozoic|Adelaide Geosyncline (West).  Age - Ediacarian in text.||||||
28299|Bunyeroo Formation|22746|6|Mentioned|p528|||||||||
28299|Bunyeroo Formation|22921|6|Mentioned|37|||Overlying unit Wonoka Formation||||||
28299|Bunyeroo Formation|22927|5|Briefly described|40|||Geol province Adelaide Geosyncline. Overlying unit Wonoka Formation, underlying unit Callana Group||||||
28299|Bunyeroo Formation|23180|4|Described|p35, Fig.1&2||Neoproterozoic|Also contains description of informal subdivision - Basal Bunyeroo Formation Dolomites (BBD)||||||
28299|Bunyeroo Formation|23211|4|Described|p41-45 Fig.2|||Informally broken into 'lower' Bunyeroo Formation. of Aruhna Subgroup.||||||
28299|Bunyeroo Formation|23250|5|Briefly described|p1124 Fig.2||Neoproterozoic III|Of Wilpena Group. Correlate of Yarloo Shale and Pertatataka Formation.||||||03-FEB-09
28299|Bunyeroo Formation|23282|6|Mentioned|p93|||||||||
28299|Bunyeroo Formation|23287|6|Mentioned|p104 Fig.2-4|||Age: Upper Ediacarian. Adelaide Geosyncline.||||||
28299|Bunyeroo Formation|23288|6|Mentioned|Fig.5|||||||||
28299|Bunyeroo Formation|23315|5|Briefly described|p345|Neoproterozoic|Neoproterozoic|Of the Wilpena Group. Shale with interbeds of limestone and dolomite.||||||07-FEB-07
28299|Bunyeroo Formation|23394|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of Wilpena Group||||||
28299|Bunyeroo Formation|23401|5|Briefly described|p575|||Overlying unit Wonoka Formation. Geological Province: Adelaide Fold Belt.||||||
28299|Bunyeroo Formation|23411|6|Mentioned|Map Legend|||||||||
28299|Bunyeroo Formation|23445|4|Described|p435|||of Wilpena Group||||||
28299|Bunyeroo Formation|23562|5|Briefly described|p295 Fig 2|Neoproterozoic III|Neoproterozoic III|||||||
28299|Bunyeroo Formation|23806|5|Briefly described|p1122 Fig. 1|Neoproterozoic|Neoproterozoic|||||||
28299|Bunyeroo Formation|23818|4|Described|p73 Fig.27, p76|Adelaidean|Adelaidean|Of the Wilpena Group. Overlying unit: Parachilna Formation. Underlying units: ABC Range Quartzite and Ulupa Siltstone. Max. thickness: 4000 ft.||||||
28299|Bunyeroo Formation|23913|4|Described|p108, p110 Fig. 2|Adelaidean|Adelaidean|Geological provice: Sturt Shelf.  Of the Wilpena Group.  Age: 588 +/- 35 Ma (Rb-Sr).  Overlying unit: Wonoka Formation.  Underlying unit: ABC Range Quartzite.||||||
28299|Bunyeroo Formation|24175|5|Briefly described|p14|Neoproterozoic|Neoproterozoic|Of the Wilpena Group.  Reddish and greenish, thin-bedded shale and siltstone.  Overlain by Wonoka Formation; overlies Brachina Formation.  Max. thickness: 1015m.||||||
28299|Bunyeroo Formation|24176|4|Described|p14, p24 Tb. 1|Adelaidean|Adelaidean|Of the Wilpena Group.  Red brown shale, minor green shale, pink limestones, dolomites. Overlain by Wonoka Formation; underlies ABC Range Quartzite.  Age is Marinoan.  Max. thickness: 1500m.  Geological Province: Mount Painter Province.  See also p27 Tb. 2.||||||11-JUN-15
28299|Bunyeroo Formation|24195|5|Briefly described|p45 Fig.3|||Parent: Aruhna Subgroup||||||
28299|Bunyeroo Formation|24321|5|Briefly described|Map legend|Late Adelaidean|Late Adelaidean|Parent: Wilpena Group||||||
28299|Bunyeroo Formation|24476|4|Described|p546, p547 Fig. 4|Vendian|Vendian|Age: c. 580 Ma. Overlies the ABC Range Quartzite. Overlain by the Wonoka Formation.  Geological Province: Adelaide fold belt.||||||
28299|Bunyeroo Formation|24481|6|Mentioned|p833|||||||||
28299|Bunyeroo Formation|24484|5|Briefly described|p803 Fig. 3|Neoproterozoic|Neoproterozoic|Unconformably overlies the Callana Beds. Overlain by the Wonoka Formation.||||||
28299|Bunyeroo Formation|24546|5|Briefly described|p2 - 3 Fig.2|Neoproterozoic|Neoproterozoic|Of Wilpena Group. Geological Province: Adelaide Fold Belt.||||||16-JAN-08
28299|Bunyeroo Formation|24586|5|Briefly described|p51 Fig. 2, p52 Fig. 3|Adelaidean|Adelaidean|Of the Aruhna Subgroup (Wilpena Group). Capped by dolostone of Wearing Dolomite.  Geological Province: Adelaide Geosyncline.||||||13-MAY-16
28299|Bunyeroo Formation|29780|5|Briefly described|p45|||||||||
28299|Bunyeroo Formation|29781|6|Mentioned|Fig.4|||||||||
28299|Bunyeroo Formation|30176|6|Mentioned|Map legend|Adelaidean|Adelaidean|Marinoan||||||
28299|Bunyeroo Formation|30177|4|Described|p90|||||||||
28299|Bunyeroo Formation|30198|6|Mentioned|p96|||||||||
28299|Bunyeroo Formation|30800|6|Mentioned|p220|||See also Fig.1.||||||
28299|Bunyeroo Formation|30801|6|Mentioned|p5|||Marinoan. Table P5-6||||||
28299|Bunyeroo Formation|30802|5|Briefly described|p12|||Marinoan age||||||
28299|Bunyeroo Formation|30807|6|Mentioned|p102|||Suggested map symbol||||||
28299|Bunyeroo Formation|31388|6|Mentioned|Fig.1|||||||||
28299|Bunyeroo Formation|31539|6|Mentioned|Fig. 6|||See also Fig. 8, 11.||||||
28299|Bunyeroo Formation|31730|6|Mentioned|p104|||Geochemical sampling - Zn anomaly||||||
28299|Bunyeroo Formation|31797|6|Mentioned|Fig. 2|||Adelaidean||||||
28299|Bunyeroo Formation|31923|6|Mentioned|p10|||||||||
28299|Bunyeroo Formation|32146|6|Mentioned|Fig.3|||||||||
28299|Bunyeroo Formation|32504|6|Mentioned|Fig.2|||||||||
28299|Bunyeroo Formation|32505|6|Mentioned|Table 3|||||||||
28299|Bunyeroo Formation|32511|6|Mentioned|Fig.1|||||||||
28299|Bunyeroo Formation|32720|6|Mentioned|Table 1|||||||||
28299|Bunyeroo Formation|32722|6|Mentioned|Fig.3|||Adelaidean. Stromatolite||||||
28299|Bunyeroo Formation|32724|6|Mentioned|Fig.1|||Marinoan. Correlation||||||
28299|Bunyeroo Formation|33036|6|Mentioned|Fig.2|||||||||
28299|Bunyeroo Formation|33037|6|Mentioned|Fig.2|||||||||
28299|Bunyeroo Formation|33474|6|Mentioned|Fig.3|||||||||
28299|Bunyeroo Formation|33655|6|Mentioned|p91|||U. Marinoan||||||
28299|Bunyeroo Formation|34069|6|Mentioned|Fig.2|||||||||
28299|Bunyeroo Formation|34175|6|Mentioned|p36|||||||||
28299|Bunyeroo Formation|34267|6|Mentioned|Fig.|||The Oraparinna & Enorama diapiric structures.||||||
28299|Bunyeroo Formation|34268|6|Mentioned|p241|||U.Prot.||||||
28299|Bunyeroo Formation|34269|6|Mentioned|Table 1|||U.Prot.||||||
28299|Bunyeroo Formation|34291|5|Briefly described|p21|||See also PP23,44,45 etc. Adelaidean||||||
28299|Bunyeroo Formation|34534|6|Mentioned|Fig.2.13|||||||||
28299|Bunyeroo Formation|34535|4|Described|p76|||Typical "red bed"||||||
28299|Bunyeroo Formation|34563|6|Mentioned|p67|||Correlation||||||
28299|Bunyeroo Formation|34598|6|Mentioned|p22|||||||||
28299|Bunyeroo Formation|34835|6|Mentioned|Fig.2|||||||||
28299|Bunyeroo Formation|34836|6|Mentioned|Fig.2|||||||||
28299|Bunyeroo Formation|34844|6|Mentioned|Fig.2|||||||||
28299|Bunyeroo Formation|34901|6|Mentioned|p18|||||||||
28299|Bunyeroo Formation|35075|6|Mentioned|Fig.2|||||||||
28299|Bunyeroo Formation|35143|6|Mentioned|Fig.2|||||||||
28299|Bunyeroo Formation|35158|6|Mentioned|p47|||||||||
28299|Bunyeroo Formation|35195|6|Mentioned|Table 3|||||||||
28299|Bunyeroo Formation|35255|6|Mentioned|Fig.6|||||||||
28299|Bunyeroo Formation|35356|5|Briefly described|p29|||Geochemistry used to locate mineralization.||||||
28299|Bunyeroo Formation|35586|6|Mentioned|p26|||||||||
28299|Bunyeroo Formation|35798|6|Mentioned|Fig.4|||Correlation of lower units in Desert Syncline drill holes.||||||
28299|Bunyeroo Formation|36083|5|Briefly described|p472|||||||||
28299|Bunyeroo Formation|36137|4|Described|p18|||See also Table 1.||||||
28299|Bunyeroo Formation|36622|6|Mentioned|Fig.2|||||||||
28299|Bunyeroo Formation|36731|6|Mentioned|p122|||Fig.3||||||
28299|Bunyeroo Formation|36898|6|Mentioned|p197|||||||||
28299|Bunyeroo Formation|37015|6|Mentioned|Fig.2|||||||||
28299|Bunyeroo Formation|37461|5|Briefly described|p343|||See also Table 5.I||||||
28299|Bunyeroo Formation|37627|6|Mentioned|p188|||||||||
28299|Bunyeroo Formation|38004|6|Mentioned|p81|||||||||
28299|Bunyeroo Formation|38022|6|Mentioned|p29|||See also Fig.4.||||||
28299|Bunyeroo Formation|38157|6|Mentioned|Table V|||||||||
28299|Bunyeroo Formation|38970|6|Mentioned|Fig.15|||||||||
28299|Bunyeroo Formation|39210|6|Mentioned|Table 4|||||||||
28299|Bunyeroo Formation|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Marinoan||||||
28299|Bunyeroo Formation|39352|6|Mentioned|Map legend|Adelaidean|Adelaidean|Marinoan||||||
28299|Bunyeroo Formation|39490|6|Mentioned|Fig.1(6)|||||||||
28299|Bunyeroo Formation|39675|6|Mentioned|Fig.2|||||||||
28299|Bunyeroo Formation|39807|6|Mentioned|p225|||||||||
28299|Bunyeroo Formation|39808|6|Mentioned|p223|||||||||
28299|Bunyeroo Formation|40455|5|Briefly described|p75|||||||||
28299|Bunyeroo Formation|40720|5|Briefly described|p55|||||||||
28299|Bunyeroo Formation|41005|6|Mentioned|p418|||||||||
28299|Bunyeroo Formation|41236|5|Briefly described|p63|||||||||
28299|Bunyeroo Formation|41401|6|Mentioned|p33|||||||||
28299|Bunyeroo Formation|41429|3|Fully described|p229|||||||||
28299|Bunyeroo Formation|41496|5|Briefly described|Fig.1|||||||||
28299|Bunyeroo Formation|41526|6|Mentioned|p14|||||||||
28299|Bunyeroo Formation|41794|6|Mentioned|p780|||||||||
28299|Bunyeroo Formation|41801|6|Mentioned|Fig.4|||||||||
28299|Bunyeroo Formation|41833|6|Mentioned|p585|||||||||
28299|Bunyeroo Formation|41953|5|Briefly described|p132|||||||||
28299|Bunyeroo Formation|42028|6|Mentioned|p137|||||||||
28299|Bunyeroo Formation|42095|5|Briefly described|p29|||See also Fig.3||||||
28299|Bunyeroo Formation|42098|5|Briefly described|Table 2 P54|||||||||
28299|Bunyeroo Formation|42101|6|Mentioned|p84|||||||||
28299|Bunyeroo Formation|42222|5|Briefly described|p19|||||||||
28299|Bunyeroo Formation|42238|5|Briefly described|Table 1 P74|||||||||
28299|Bunyeroo Formation|42240|6|Mentioned|Fig.2 P165|||||||||
28299|Bunyeroo Formation|42241|4|Described|p181|||||||||
28299|Bunyeroo Formation|42272|5|Briefly described|p403|||||||||
28299|Bunyeroo Formation|42357|5|Briefly described|p10|||||||||
28299|Bunyeroo Formation|42546|5|Briefly described|Map legend|Adelaidean (Marinoan)||||||||
28299|Bunyeroo Formation|42600|5|Briefly described|p10|||||||||
28299|Bunyeroo Formation|42736|5|Briefly described|map legend|Neoproterozoic||||||||
28299|Bunyeroo Formation|42763|5|Briefly described|p22|||see also Fig.2 P21||||||
28299|Bunyeroo Formation|42777|5|Briefly described|p292|||||||||
28299|Bunyeroo Formation|42779|5|Briefly described|p283|||||||||
28299|Bunyeroo Formation|42813|6|Mentioned|p22|||of Wilpena Group||||||
28299|Bunyeroo Formation|43052|5|Briefly described|p194,table 6.1|||Of Wilpena  Group.||||||03-FEB-09
28299|Bunyeroo Formation|43595|5|Briefly described|p547|||||||||
28299|Bunyeroo Formation|43622|6|Mentioned|p38|Neoproterozoic||||||||
28299|Bunyeroo Formation|43650|5|Briefly described|p444||Neoproterozoic|||||||
28299|Bunyeroo Formation|43651|6|Mentioned|p438|||||||||
28299|Bunyeroo Formation|43673|6|Mentioned|p374|||Ejecta age: approx. 0.59 Ga||||||
28299|Bunyeroo Formation|43845|5|Briefly described|Fig3 p43, 44,46||Neoproterozoic|In Wilpena Group.||||||12-JUL-16
28299|Bunyeroo Formation|44133|6|Mentioned|p59|||||||||
28299|Bunyeroo Formation|44659|5|Briefly described|map legend|||Marinoan, lithology.||||||
28299|Bunyeroo Formation|44660|14|Not recorded|map legend|||Marinoan, lithology.||||||
28299|Bunyeroo Formation|44689|14|Not recorded|map legend|||Andamooka. (H53-12). Unit of Wilpena Group. Marinoan.||||||
28299|Bunyeroo Formation|46865|6|Mentioned|Table 2|||||||||
28299|Bunyeroo Formation|50127|6|Mentioned|p48|||Geological Province: Stuart Shelf.||||||27-MAY-04
28299|Bunyeroo Formation|60418|5|Briefly described|p134 Fig.1|Neoproterozoic|Neoproterozoic|Of Wilpena Group.||||||
28299|Bunyeroo Formation|60889|6|Mentioned|p250 Fig.7|||||||||
28299|Bunyeroo Formation|60955|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Yarloo Shale equivalent. Of the Wilpena Group. Red and minor green micaceous shales.||||||13-APR-05
28299|Bunyeroo Formation|60959|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Of the Wilpena Group. Brick red shale. Includes 10-30 mm thick layer of felsic subrounded volcanics.||||||13-MAY-16
28299|Bunyeroo Formation|61236|5|Briefly described|p23, 24 Fig. 1|Adelaidean|Adelaidean|Includes volcanic rock fragments within red mudstone.||||||14-MAY-07
28299|Bunyeroo Formation|61308|5|Briefly described|p7|Proterozoic|Proterozoic|Shale - distinctive maroon colour with greenish layers.||||||
28299|Bunyeroo Formation|61560|5|Briefly described|p498 Tb. 4|||Contains confirmed Acraman impact ejecta. In the Flinders Ranges. See also p500.||||||13-MAY-16
28299|Bunyeroo Formation|61565|5|Briefly described|p607|Neoproterozoic III|Neoproterozoic III|Contains ejecta horizon from the Acraman-Bunyeroo impact event. Age: 550Ma (Rb-Sr whole rock shale). Geological Province: Gawler Craton.||||||03-FEB-09
28299|Bunyeroo Formation|61732|3|Fully described|p5 Tb. 1, p44-46|Marinoan|Marinoan|Of Wilpena Group. Overlies ABC Quartzite disconformably. Max. thickness in type section: 700m. Geol.Prov: Adelaide Rift Complex/Stuart Shelf. See also p28 Fig. 13, p134.||||||07-FEB-11
28299|Bunyeroo Formation|62085|6|Mentioned|p19 Fig.4, p20, p25|Ediacaran|Ediacaran|||Unit in Wilpena Group.|||Mudstone, with impact debris layer.|
28299|Bunyeroo Formation|62428|5|Briefly described|p351 Tb. 6|Neoproterozoic III|Neoproterozoic III|Age: 588+/35Ma (Rb-Sr). Palaeomagnetic data.||||||10-FEB-09
28299|Bunyeroo Formation|62592|5|Briefly described|p50 Table 5.1.|Ediacaran|Ediacaran|Adelaide Geosyncline.||Unit in Wilpena Group.||Disconformably overlies Sandison Subgroup.|Fine siltstone; impact debris layer.|
28299|Bunyeroo Formation|62784|5|Briefly described|p8 Fig.1|Neoproterozoic|Neoproterozoic|Of Wilpena Group. Includes Wilcolo Sandstone Member.||||||
28299|Bunyeroo Formation|62869|6|Mentioned|p631 Fig. 6|||||||||
28299|Bunyeroo Formation|62903|6|Mentioned|p730 Fig.1|||Adelaide Rift Complex. Presented in figure as Bunyeroo.||||Overlies ABC Range Quartzite; is overlain by Wonoka Formation||13-MAY-16
28299|Bunyeroo Formation|62962|5|Briefly described|p2296 Tab. 6|||Thickness: 3300m, estimated. Geological Province: Mount Painter Province. Sandstone and quartzite.||||||07-FEB-11
28299|Bunyeroo Formation|63458|6|Mentioned|p897 Fig.19. |Ediacaran|Ediacaran|||Unit in Wilpena Group.||||
28299|Bunyeroo Formation|64068|5|Briefly described|p8|||Adelaide Rift. Schmidt and Clark (2000) postulate two reversals, in rapid succession, of Australia's plate motion around 575 Ma, based on a single paleopole from this unit.||||||
28299|Bunyeroo Formation|64455|5|Briefly described|p137|Neoproterozoic III|Neoproterozoic III|Of Wilpena Group. Includes Wilcolo Sandstone Member. Underlies Wonoka Formation. Mauve or grey laminated siltstone. Age is Ediacaran.||||||
28299|Bunyeroo Formation|64794|6|Mentioned|p254|||Adelaide Rift Complex.||||Coeval with Dey Dey Mudstone.|Includes black shales.|
28299|Bunyeroo Formation|64797|6|Mentioned|p153 Fig.2, p164 Fig.11, p169 Fig.12|Ediacaran|Ediacaran|Adelaide Rift Complex. Lithology/rank not shown on diagram.||||||
28299|Bunyeroo Formation|64829|5|Briefly described|p1084-5 Figs.1,  2|Neoproterozoic|Neoproterozoic|||||||07-FEB-11
28299|Bunyeroo Formation|65313|6|Mentioned|p576 Fig. 5|Neoproterozoic|Neoproterozoic|||||||
28299|Bunyeroo Formation|65410|6|Mentioned|p74.|||Adelaide Geosyncline. Part of Supersequence 3.||||||
28299|Bunyeroo Formation|65892|4|Described|p16, p32-33, p35, p38-39.  |Ediacaran|Ediacaran|Flinders Ranges. Last major Neoproterozoic transgression, reaching the Stuart Shelf but not the eastern Curnamona Province. Has a distinctive layer of iridium-rich sandstone with boulder-sized clasts; ascribed to Acraman bolide impact.|c.580 Ma.|Unit in Wilpena Group.||Overlies ABC Range Quartzite. Is overlain by Wonoka Formation.|Red shale and siltstone.|
28299|Bunyeroo Formation|65922|6|Mentioned|p10, 32|Late Neoproterozoic|Late Neoproterozoic|Shock metamorphosed material has been found within this Formation. Some authors argue that the material was formed as a result of a bolide impact structure at ~600 Ma which also produced the nearby Lake Acraman.||||||
28299|Bunyeroo Formation|65925|5|Briefly described|Appendix 2.||||||||Siltstone, shale, grey-red to grey-green, partly calcitic, minor fine grained sandstone; dolomite, grey; limestone, grey, lenses, thin beds.|
28299|Bunyeroo Formation|66569|4|Described|p859, p860, p861 fig.2, p861,|Ediacaran|Ediacaran|Of Wilpena Group; correlated with Dey Dey Mudstone; marine mudstone with lonestones; contains an Acraman impact ejecta horizon; underlies Wonoka Formation; overlies ABC Range Quartzite; equivalent to Yarloo Shale; 593+/-32 Ma||||||29-APR-16
28299|Bunyeroo Formation|67030|5|Briefly described|p409,  Fig. 2, p412 Fig.7, p413 Tab. 3|Ediacaran|Ediacaran|Magnetic information presented for comparison (Schmidt & Williams 1996). Abbreviated as Bunyeroo Fm in Fig. 2 and Tb. 2||||Overlies the ABC Quartzite, underlies the Wonoka Formation; equivalent to the Yarloo Shale.||26-APR-12
28299|Bunyeroo Formation|67484|6|Mentioned|p294 Tb.1|Ediacaran|Ediacaran|Adelaide Rift Complex.||Of the Wilpena Group.||Overlain by Wonoka Formation. Underlain by ABC Range Quartzite.||
28299|Bunyeroo Formation|67620|5|Briefly described|p5|Ediacaran|Ediacaran|Adelaide Rift Complex.||Wilpena Group.||Overlies ABC Range Quartzite. Is overlain by Wonoka Formation.||
28299|Bunyeroo Formation|67870|5|Briefly described|p9|Ediacaran|Ediacaran|Adelaide Rift System.||Wilpena Group.||||
28299|Bunyeroo Formation|68030|4|Described|p238-240|Ediacaran|Ediacaran|Flinders Ranges. Deepwater deposition during maximum sea level.  ||Unit of Wilpena Group.|Includes Bunyeroo red beds and Wilcolo Sandstone Member.|Overlain by Weaing Dolomite Member. Underlain unconformably by ABC Range Quartzite.|Maroon, laminated siltstone with apparent cyclic bedding. Local onlapping breccias near diapirs.|
28299|Bunyeroo Formation|68138|6|Mentioned|p156|Neoproterozoic|Neoproterozoic|Adelaide Rift Complex.||Wilpena Group.||||
28299|Bunyeroo Formation|68269|5|Briefly described|p673-674|Ediacaran|Ediacaran|Adelaide Geosyncline, widespread. c. 400-m-thick. Grades upward into outer marine-shelf mudstone. Contains a ca 25-cm-thick impact ejecta horizon of dacitic fragments 80 m above the base of the unit (serves as a marker horizon); this is overlain and underlain by anomalous coarse-grained deposits interpreted as ice-rafted detritus (dropstones, dumps and frozen aggregates). Unit was deposited during thermal subsidence phase of Adelaide Geosyncline. Deformed during the 514-490 Ma Delamerian orogeny. Age of 593 +/- 32 Ma is from Rb-Sr whole-rock shale dating and c. 580 Ma is based on chemostratigraphic correlations.|593+/- 32 Ma, c. 580 Ma|Wilpena Group|Wilcolo Member|Underlain by ABC Range Quartzite. Overlain by Wonoka Formation. Correlates to Dey Dey Mudstone.|Red, laminated and fissile, hemipelagic mudstone.|
28299|Bunyeroo Formation|68271|6|Mentioned|p696-697|||Brief chemostratigraphy (Delta34S) provided on pyrites in the Bunyeroo Fm.||||||
28299|Bunyeroo Formation|68274|6|Mentioned|p13|Neoproterozoic|Neoproterozoic|||||||
28299|Bunyeroo Formation|68277|6|Mentioned|p103|Neoproterozoic|Neoproterozoic|May have been glaciated in the mid-Ediacaran interval (Jenkins, 2011).||||||
28299|Bunyeroo Formation|68473|6|Mentioned|p531|||Adelaide Rift Complex.||||||
28299|Bunyeroo Formation|69019|3|Fully described|p56-57 Pl.9, p58.|Ediacaran|Ediacaran|Defined by Dalgarno and Johnson (in Thomson et al. 1964); revised by Gostin and Jenkins (1983) to exclude the Wearing Dolomite Member. Type section in Brachina Creek where it is 700 m thick. Regionally, hosts a thin but persistent layer of coarse tuff-like feldspathic detritus, interpreted as ejecta blanket from the Acraman bolide impact on the Gawler Craton. Poorly defined Rb-Sr whole rock isochron age from Yarloo Shale (equivalent unit on the Stuart Shelf).|588 +/- 35 Ma (?Webb, 1980).|Unit in Wilpena Group.||Overlies Ulupa Siltstone; unconformably overlies ABC Range Quartzite. Is overlain unconformably by Cadna-owie Formation, and conformably by Wonoka Formation.|Grey-red to grey-green siltstone and shale, partly calcareous; weathers to a distinct red; minor fine-grained sandstone beds; grey dolomite and limestone occur as lenses and thin beds.|
28299|Bunyeroo Formation|70031|5|Briefly described|p243,245,250|Ediacaran|Ediacaran|Adelaide Geosyncline. Depositional environment: marine shelf. Contains ice-rafted detritus in the lower part of the section indicating a third, Ediacaran episode during the late Neoproterozoic. Ca. 590 Ma date for late Cryogenian to post-Delamerian Orogeny poles. See p250 Table 2 for paleomagnetic analysis.||Unit of Wilpena Group.||Overlain by Wonoka Formation. Underlain by ABC Range Quartzite.||
28299|Bunyeroo Formation|70082|6|Mentioned|p2-3|Ediacaran|Ediacaran|Flinders Ranges. Contains red beds and marine till. Contains glacial dropstone with glaciation dated by U-Pb at 582+\-4 Ma.||||||
28299|Bunyeroo Formation|70323|6|Mentioned|p221|||Adelaide Geosyncline. Contains moderately iron-oxide-rich sediments.||||||
28299|Bunyeroo Formation|70333|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic||||||Siltstone, shale, grey-red to grey-green, partly calcitic, minor fine-grained sandstone; dolomite, grey; limestone, grey, lenses, thin beds.|
28299|Bunyeroo Formation|70334|5|Briefly described|p2,20,30,36-37,65,78|Ediacaran|Ediacaran|Geological province: Gawler Craton. Of Adelaide Geosyncline. Transgressive deposit, subtidal-mudflat environment during widespread flooding over Adelaide Geosyncline and Stuart Shelf. Deeply incised, forming major canyons. Deposited in a marine setting below storm wave base in the middle to outer shelf (Haines, 1990), and  represents a rapid marine transgression following the deposition of the ABC Range Quartzite (Preiss, 1987). Two main hypotheses for canyon incision: a) canyons cut by fluvial processes following base level change produced by tectonic uplift or Messinian-style sea level change and filled by coastal onlap, or b)  cut in an entirely marine environment (see p37,78 for details).||Unit of Wilpena Group.|||Purple-red to grey-green siltstone containing minor grey-green finegrained sandstone beds.|14-OCT-19
28299|Bunyeroo Formation|70384|5|Briefly described|Map legend.|Ediacaran|Neoproterozoic|Adelaide Geosyncline. Appears tio be shown as part o fan unnamed subgroup, Wilpena Group.|||||Grey-red to grey-green siltstone, shale, partly calcareous; minor fine-grained sandstone beds; grey dolomite and limestone as lenses and thin beds.|23-JAN-19
28299|Bunyeroo Formation|70406|5|Briefly described|p125, 128|||Outcrop at Ochre Cove now identified as Corraberra Sandstone Member of Brachina Formation.||Of Aruhna Subgroup.||||
28299|Bunyeroo Formation|70407|4|Described|p108-109, 102, 103, 105, 106, 112, 113|Neoproterozoic|Neoproterozoic|Age: Ediacaran. 700m thick in type section at Brachina Gorge. Thickens eastward of Torrens Hinge Zone. Mostly deposited below storm wave base. Mid to outer shelf setting.||Of Aruhna Subgroup.||Overlain by Wearing Dolomite.|Laminated to massive, dark reddish brown shale in type section.|
28299|Bunyeroo Formation|70790|5|Briefly described|p258 Fig.1, p259|Ediacaran|Ediacaran|Adelaide Rift Complex.|||||Mainly carbonate mudstones.|
28299|Bunyeroo Formation|71237|14|Not recorded|p10, 17|||||||||
28299|Bunyeroo Formation|71241|2|Defined|p13, 14, 17, p9-10|||||Of Wilpena Group.||Gradational contact with overlying Wonoka Formation in type section.||
28299|Bunyeroo Formation|71250|6|Mentioned|p70|Ediacaran|Ediacaran|Central Flinders Ranges.||Wilpena Group.||Overlies ABC Range Quartzite. Is overlain by Wearing Dolomite Member (Wonoka Formation).||
28299|Bunyeroo Formation|71288|6|Mentioned|p140|Neoproterozoic|Neoproterozoic|||||||
28299|Bunyeroo Formation|72449|5|Briefly described|p1, p2 Map Legend|Neoproterozoic|Neoproterozoic|Deposited in deep, quiet water. Includes Acraman impact layer.||||Overlies ABC Range Quartzite and underlies Wonoka Formation.|Red-brown shale with thin, gritty sandstone, sometimes conglomeratic at base. Thin light green bands and small spherical reduction spots are common. Acraman ejecta debris layer occurs approximately 80 m above base.|
28299|Bunyeroo Formation|72450|5|Briefly described|Brochure map|||||Wilpena Group|||Maroon, fine-grained siltstone.|
28299|Bunyeroo Formation|72451|4|Described|p4|Late Proterozoic|Late Proterozoic|Represents a rapid marine transgression inundating the underlying ABC Range Quartzite (Preiss, 1987). Mostly deep marine, but sandier and stromatolitic horizons in upper part indicate shallow nvironment.||||Overlies ABC Range Quartzite. Is overlain by Wonoka Formation.|Red brown shale and siltstone with minor fine sandy layers.|
28299|Bunyeroo Formation|72456|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Marree 1:250k map sheet. |||||Siltstone, shale, grey-red to grey-green, partly calcitic, minor fine-grained sandstone; dolomite, grey; limestone, grey, lenses, thin beds.|09-JUN-22
28299|Bunyeroo Formation|73086|6|Mentioned|p122|||Adelaide Rift Complex.||||Correlates to Pertatataka Formation.||
28299|Bunyeroo Formation|73110|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic||||||Siltstone, shale, grey-red to grey-green, partly calcitic, minor fine-grained sandstone; dolomite, grey; limestone, grey, lenses, thin beds.|
28299|Bunyeroo Formation|73188|5|Briefly described|p315-316, p331, p334-335, p346, p353|Ediacaran|Ediacaran|Mount Lofty Ranges.||Wilpena Group||[Disconformably?] overlain by Normanville Group. Unconformably overlain by Ochre Cove Formation.|Red mudstone.|
28299|Bunyeroo Formation|73222|5|Briefly described|p6, p8, p11-12, p14, p16, p18-21, p23-26|Ediacaran|Ediacaran|Adelaide Rift Complex. [Article includes O and C stable isotope investigation].||Aruhna Subgroup, Wilpena Group, Heysen Supergroup||||
28299|Bunyeroo Formation|73236|6|Mentioned|p40|Ediacaran|Ediacaran|Exposed near Ochre Point.||||Underlain by ABC Range Quartzite.|Red mudstone.|
28299|Bunyeroo Formation|73255|6|Mentioned|p534 Fig.2|Ediacaran|Ediacaran|Contains Acraman ejecta layer.|ca 578 Ma|||Overlies the ABC Quartzite, underlies the Wonoka Formation.||
28299|Bunyeroo Formation|74367|5|Briefly described|p7 Fig.6, p9, p11, p14, p17, p19-20, p22|||Adelaide Rift Complex. MDA of 1041+/-26 Ma is significantly older than the true depositional age. Additional depositional age of 593+/-32 Ma (Compston et al., 1987).||Aruhna Subgroup, Wilpena Group||Equivalent to Yarloo Shale||
82226|Burden Metagabbro|73230|2|Defined|p6, p9-10, p12-16|Siderian|Siderian|New name [see appendix and ASUD for definition]. Gawler Craton. Domain: Christie and Wilgena. Previously included in the Aristarchus Peridotite. Nickel mineralisation has not been intersected. Known from lithostratigraphic correlations to be older than Aristarchus Metaperidotite. Named after Burden Tank on the TARCOOLA mapsheet. Type locality: drillhole DMDD-002 (234168), interval 96-318 m (total depth). Occurs in drillholes near Aristarchus Paddock in the southern Christie Domain. Thickness: occurs over greater than 220 m in type drillhole with individual layers 0.05 to over 2 m thick. Magmatic age [also written as c. 2490 Ma] is zircon SHRIM U-Pb from Reid et al. (2014). Temporal correlative of the Mobella Tonalite.|c. 2488 Ma (magmatic)|Mulgathing Complex||Intrudes Christie Gneiss. Intruded by Aurora Tank Suite and Aristarchus Metaperidotite.|Gabbroic gneiss with plagioclase, hornblende and possible magnetite. Poikioblastic hornblende with abundant plagioclase inclusions (former pyroxene).|
27124|Burnham Limestone|22525|6|Mentioned|p35,37,38||Pleistocene|||||||
27124|Burnham Limestone|22541|5|Briefly described|p 37|||||||||
27124|Burnham Limestone|22941|5|Briefly described|p290||Early Pleistocene|Basal unit of the Seaford Formation.||||||
27124|Burnham Limestone|23489|4|Described|p45|Pliocene|Pliocene|||||||
27124|Burnham Limestone|23887|5|Briefly described|p203|Early Pleistocene|Early Pleistocene|||||||
27124|Burnham Limestone|24102|5|Briefly described|p132|Early Pleistocene|Early Pleistocene|Age: ~1.7 Ma.||||||30-NOV-04
27124|Burnham Limestone|24566|5|Briefly described|p111|Early Pleistocene|Early Pleistocene|Age: ca1.7Ga. Geological Province: Saint Vincent Basin.||||||03-MAY-05
27124|Burnham Limestone|30757|2|Defined|p2|Pleistocene|Pleistocene|||||||
27124|Burnham Limestone|35689|6|Mentioned|Plate 7|||||||||
27124|Burnham Limestone|38107|6|Mentioned|Table 1|||See also p19.||||||11-NOV-22
27124|Burnham Limestone|38699|6|Mentioned|p29|||||||||
27124|Burnham Limestone|38700|4|Described|p38|||||||||
27124|Burnham Limestone|39351|6|Mentioned|Map legend|Quaternary|Quaternary|||||||
27124|Burnham Limestone|39522|6|Mentioned|p86|||||||||
27124|Burnham Limestone|39835|6|Mentioned|p284|||||||||
27124|Burnham Limestone|40442|6|Mentioned|p35|||See also Fig.20.||||||
27124|Burnham Limestone|40453|6|Mentioned|p61|||||||||
27124|Burnham Limestone|41025|6|Mentioned|Fig.1|||||||||
27124|Burnham Limestone|41513|5|Briefly described|Fig.5|||See also p40||||||11-NOV-22
27124|Burnham Limestone|42733|6|Mentioned|map legend|Tertiary||||||||
27124|Burnham Limestone|43682|6|Mentioned|p290||Pleistocene|||||||
27124|Burnham Limestone|44133|5|Briefly described|p68, 170, 222, 165 Fig. 10.11|Pliocene|Pliocene|Geological Province: Saint Vincent Basin. Overlies: Hallet Cove Sandstone. ||||||
27124|Burnham Limestone|61155|5|Briefly described|p17|Pleistocene|Pleistocene|Partly overlies Hallett Cove Sandstone. Geological Province: St Vincent Basin.||||||
27124|Burnham Limestone|65375|4|Described|pp38-40.|Quaternary|Quaternary|Name given to a c.1.5m thick unconsolidated skeletal limestone at Browns Beach, equivalent to Point Ellen Limestone.||||Unconformably overlies Gleesons Landing Granite. Is unconformably overlain by Bridgewater Formation.|Unconsolidated skeletal limestone with abundant fragments of coral, bivalves, bryozoans and brackish-water foraminifers.|
27124|Burnham Limestone|65901|5|Briefly described|p176, p176 Tab.1|Pleistocene|Pleistocene|Interfingers with Seaford Formation. Marine fossils suggest earliest Pleistocene age.||||||08-MAR-12
27124|Burnham Limestone|66131|6|Mentioned|p242 Fig.2|Pleistocene|Pliocene|Late Pliocene to Pleistocene in age (from p.242 Fig.2 - stratigraphic correlation chart).||||||
27124|Burnham Limestone|67462|5|Briefly described|Map legend.|Pliocene|Pliocene|Eastern Saint Vincent Basin.||||Overlies Hallett Cove Sandstone.||
27124|Burnham Limestone|68715|6|Mentioned|p31 Fig.5|Pliocene|Pliocene|St Vincent Basin. Early Pliocene age.||||||
27124|Burnham Limestone|70660|5|Briefly described|p3, p9-p10, p12|Early Pleistocene|Early Pleistocene|NB: age is uncertain. See also p20, p21 fig 11c, p29, p32, p40.||||Overlies the Hallett Cove Sandstone. Overlain by the Ochre Cove Formation. Equivalent to the Point Ellen Limestone.|Limestone, fine-grained and poorly fossiliferous.|
27124|Burnham Limestone|72450|5|Briefly described|Brochure, Brochure map|Pleistocene|Pleistocene|||||||
27124|Burnham Limestone|73188|5|Briefly described|p319-320, p331, p346, p351, p357, p359|Pleistocene|Pleistocene|St Vincent Basin. Shallow marine.||||Underlain by Hallett Cove Sandstone and Seaford Formation. Overlain by Ochre Cove Formation.||
27124|Burnham Limestone|73236|6|Mentioned|p43|Pleistocene|Pliocene|Occurs at Marino Rocks.||||Overlain by Ochre Cove Formation.||
30306|Burr Well Member|24586|5|Briefly described|p52|||Of the Wearing Dolomite.||||||05-JUL-06
30306|Burr Well Member|43845|6|Mentioned|p45,46||Neoproterozoic|Member of Wearing Dolomite||||||12-JUL-16
30306|Burr Well Member|68713|6|Mentioned|p19|||||Of the Wonoka Formation.||||
30306|Burr Well Member|69019|5|Briefly described|p58-59, p166.|||1 to 5 m thick.||Unit in Wonoka Formation.|||Locally laminated, white dolomicrite that weathers to buff or brown hues.|
30306|Burr Well Member|70384|5|Briefly described|Map legend.|Ediacaran|Neoproterozoic|Adelaide Geosyncline. Forms a lining on walls of submarine canyons.||Of Wonoka Formation.|||White dolomicrite, 1-5m thick, buff to brown weathering, locally laminated; forms a lining on walls of submarine canyons.|23-JAN-19
30306|Burr Well Member|70407|4|Described|p103 Fig 2, p109 Fig 11, p110|Neoproterozoic|Neoproterozoic|Age: Ediacaran. Deposited in storm-dominated shoreface to tide-dominated lagoonal environment.||Of Wearing Dolomite. Of Di Bona (1989) unpub PhD.|||Mature, medium-grained, swaley cross-stratified, carbonate-cemented sandstone or intraformational conglomerate with edgewise clasts of dolostone.|
30306|Burr Well Member|72456|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Marree 1:250k map sheet. |||||Dolomicrite, white, buff-brown-weathering, massive, locally laminated comprising condensend sequences of shale with dolomicrite hardgrounds on top.|09-JUN-22
34321|Bute Metadolerite|22629|6|Mentioned|p153|Proterozoic|Proterozoic|Formerly Bute Amphibolite||||||
34321|Bute Metadolerite|24475|2|Defined|p56|Mesoproterozoic|Mesoproterozoic|Formerly Bute Amphibolite.  Intrudes Wandearah Metasediments.||||||
34321|Bute Metadolerite|60958|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Dolerite and diorite intrusives in the Bute region. Mainly medium to fine-grained plagioclase and hornblende, minor quartz, biotite, epidote, chlorite and opaques.Geological Province: Gawler Craton.||||||
34321|Bute Metadolerite|61121|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Dolerite and diorite intrusives in the Bute region. Mainly medium- to fine-grained  plagioclase and hornblende, minor quartz, biotite, epidote, chlorite and opaques. Occasionally ophitic textures. Geological Province: Gawler Craton.||||||02-JUN-05
34321|Bute Metadolerite|63398|5|Briefly described|p669, p670 Fig. 6d|Mesoproterozoic|Mesoproterozoic|Age: ?1580Ma. Mafic rocks. ||||||
34321|Bute Metadolerite|65376|6|Mentioned|p101 Fig.3.1.|||||||||
34805|Byilkaoora Member|22922|6|Mentioned|p33|Ordovician|Ordovician|Of Mount Chandler Sandstone.||||||
34805|Byilkaoora Member|23282|1|Redefined|p81||Late Ordovician|Originally basal part of Mount Chandler Sandstone, the unit was defined as the Byilkaoora Formation of Benbow (1982). Now redefined as a member of Mount Chandler Sandstone, Officer Basin. Age: Late Ordovician 457-455Ma.||||||
34805|Byilkaoora Member|24112|5|Briefly described|p254 Fig.2|Late Ordovician|Early Ordovician|Of the Munda Group. Geological Province: Officer Basin.||||||07-SEP-18
34805|Byilkaoora Member|72478|6|Mentioned|p8|Late Ordovician|Early Ordovician|Officer Basin.||Mount Chandler Sandstone.||||25-MAR-21
31517|Cadell Formation|23179|6|Mentioned|p32, Fig.2||Middle Miocene|Parent: Morgan Group, gp:Murray Basin.||||||
31517|Cadell Formation|23226|2|Defined|p899||Balcombian|Was Cadell Marl lens and Cadell Marl Member. Status raised to formation acknowledging distinct litho and faunal attributes relative to its bounding strata. Of Morgan Group.||||||
31517|Cadell Formation|23768|5|Briefly described|p34|||Also referred to as Cadell Marl.||||||30-MAR-05
31517|Cadell Formation|24558|4|Described|p655 Fig. 3|Middle Miocene|Middle Miocene|Low energy carbonate ramp sediments with with abundant molluscs. Conformably overlies Glenforslan Formation; conformably overlain by Bryant Creek Formation.||||||11-APR-05
31517|Cadell Formation|63460|5|Briefly described|p839 Fig. 2b, p848|Middle Miocene|Middle Miocene|of the Morgan Group. Overlies Glensforlan Formation. Overlain by Bryant Creek and Pata Formations. Geological province: Murray Basin. Clay/marl unit.||||||
31517|Cadell Formation|64237|5|Briefly described|p18 Fig.2|Middle Miocene|Middle Miocene|Formerly Cadell Marl Lens (Lawrence 1961)); revised to Cadell Marl Member (Rogers et al 1995) then Cadell Formation (Lukasik and James 1998) in their revision of Murray Gp up to Murray Supergroup. The name, Cadell Fm, retained in Murray Gp+2 Mbrs.||||||28-JAN-09
31517|Cadell Formation|68715|5|Briefly described|p31 Fig.5|Miocene|Miocene|Murray Basin. Middle Miocene age.||Of the Murray Group.||||
31517|Cadell Formation|72445|5|Briefly described|App.6 p2 Fig.1.|Middle Miocene|Middle Miocene|Of Gallagher and Gourlay (2007), Lukasik and James (1998). See also Cadell Marl App.7.||Murray Supergroup||Underlies Pata and Bryant Creek Formation|Includes marl and marly limestone.|
31517|Cadell Formation|73228|6|Mentioned|p50, p55-57|Middle Miocene|Late Early Oligocene|Murray Basin.||Murray Group||||
31517|Cadell Formation|73229|6|Mentioned|p67|Middle Miocene|Late Early Oligocene|Murray Basin.||Murray Group||||
26296|Cadlareena Volcanics|22589|6|Mentioned|p129||Cryogenian|part of the Arkaroola Subgroup||||||
26296|Cadlareena Volcanics|22746|5|Briefly described|Fig.3 p515|Cryogenian|Cryogenian|||||||
26296|Cadlareena Volcanics|22922|5|Briefly described|33|||||||||
26296|Cadlareena Volcanics|23054|5|Briefly described|p10-11,33|||||||||
26296|Cadlareena Volcanics|23282|2|Defined|p53||Neoproterozoic|Age: Precambrian, Neoproterozoic, Willouran to Tourensian Epochs. of Ambrose et al (1981). Equiv. to Wooltana and Boucaut Volcanics and Kilroo Formation. Age of equiv: (BV) 783 +/- 42Ma, (Kilroo) 768+/_9 & 764+/-42Ma.||||||
26296|Cadlareena Volcanics|23288|6|Mentioned|p128 Fig.5,18|||of Central and Eastern Officer Basin.||||||
26296|Cadlareena Volcanics|24112|5|Briefly described|p254 Fig.2|Neoproterozoic|Neoproterozoic|Geological Province: Officer Basin||||||
26296|Cadlareena Volcanics|24175|6|Mentioned|p8|||||||||
26296|Cadlareena Volcanics|24506|5|Briefly described|p16|Neoproterozoic|Neoproterozoic|Mafic volcanics.  Age is Adelaidean.||||||19-SEP-05
26296|Cadlareena Volcanics|36733|2|Defined|p68|early Adelaidean|early Adelaidean|See also P26.||||||
26296|Cadlareena Volcanics|37854|6|Mentioned|p9|||See also Table 1.||||||
26296|Cadlareena Volcanics|38108|6|Mentioned|Table 1|||||||||
26296|Cadlareena Volcanics|38157|6|Mentioned|Table II|||||||||
26296|Cadlareena Volcanics|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Willouran||||||
26296|Cadlareena Volcanics|39352|6|Mentioned|Map legend|Adelaidean|Adelaidean|Willouran||||||
26296|Cadlareena Volcanics|40294|6|Mentioned|p29|||See also Table 2||||||
26296|Cadlareena Volcanics|41403|3|Fully described|p52|||||||||
26296|Cadlareena Volcanics|42223|4|Described|p34|||See also Table 1||||||
26296|Cadlareena Volcanics|42224|6|Mentioned|p51|||||||||
26296|Cadlareena Volcanics|42235|6|Mentioned|p142|||||||||
26296|Cadlareena Volcanics|42238|6|Mentioned|p71|||||||||
26296|Cadlareena Volcanics|43052|5|Briefly described|p172,Table 6.2|||of Arkaroola Subgroup||||||
26296|Cadlareena Volcanics|43743|6|Mentioned|Fig.2,p33||Neoproterozoic|||||||
26296|Cadlareena Volcanics|44289|5|Briefly described|Map Legend||Neoproterozoic|||||||
26296|Cadlareena Volcanics|62453|6|Mentioned|p13|||Correlated with the Wooltana Volcanics||||||
26296|Cadlareena Volcanics|63397|6|Mentioned|5|||||||||
26296|Cadlareena Volcanics|64625|6|Mentioned|p246|||Officer Basin. Probably fed by the Gairdner Dyke Swarm.||||||
26296|Cadlareena Volcanics|64794|6|Mentioned|p238 fig 2|Cryogenian|Cryogenian|||||||
26296|Cadlareena Volcanics|64796|6|Mentioned|p183 fig.2, p200 Fig.10|||Of Officer Basin||||||
26296|Cadlareena Volcanics|65363|5|Briefly described|p8, p37.|Neoproterozoic|Neoproterozoic|Possible correlative of Keene Basalt in Western Australia.|780 - 760 Ma (Morton 1997).|||||
26296|Cadlareena Volcanics|65365|5|Briefly described|p10|Cryogenian|Cryogenian|Eastern Officer Basin. Possible correlative of Wooltana Volcanics.||||||19-MAR-12
26296|Cadlareena Volcanics|69666|6|Mentioned|p24, p26, p36|Neoproterozoic|Neoproterozoic|Peake and Denison Inlier. Part of the Willouran Basic Province.||||||
26296|Cadlareena Volcanics|70334|5|Briefly described|p45|Tonian|Tonian|Geological province: Gawler Craton. Of Adelaide Geosyncline. Part of the Willouran Basic Province. Emplaced during a major NE-SW extensional event, which was followed by continental rifting and the break-up of the supercontinent Rodinia (Crawford and Hilyard, 1990, Zhao et al., 1994, Li et al., 1999, Wang et al., 2010).||||||
26296|Cadlareena Volcanics|71129|5|Briefly described|p103|Tonian|Tonian|Geological Province: Gawler Craton. Of Adelaide Geosycline. Part of the Willouran Basic Province, which also includes Beda Basalt, and the Wooltana and Noranda volcanics, Wilangee Basalt, Little Broken Hill Gabbro and Gairdner Dolerite. Related to the Rodinian break-up (Zhao et al., 1994, Li et al., 1999, Wang et al., 2010). Basaltic volcanism interpreted to be result of mantle plume upwelling, causing doming in the continental lithosphere (Zhao et al., 1994).||||||
26296|Cadlareena Volcanics|72478|6|Mentioned|p8|Willouran|Torrensian|Officer Basin.|c. 780-760 Ma|Callanna Group||Overlies the Coominaree Dolomite.||24-MAR-21
26296|Cadlareena Volcanics|74367|6|Mentioned|p18|||Willouran Basic Province. Suggested to be coeval with Gairdner Dolerite (827+/-6 Ma, Wingate et al., 1998).||||Correlated with Wooltana Volcanics||
34977|Cadney Park Member|22922|5|Briefly described|33 fig 2|Early Cambrian|Early Cambrian|Of Observatory Hill Formation, Officer Basin.||||||30-JUN-14
34977|Cadney Park Member|23282|2|Defined|p73||Early Cambrian|Age: Early Cambrian 524 - 522Ma. of Officer Basin. Informally used for years as 'Cadney Park' Formation, and now defined as a member of Observatory Hill Formation.||||||10-AUG-07
34977|Cadney Park Member|62570|5|Briefly described|p580 Figs. 2 and 3|Middle Cambrian|Middle Cambrian|Of Observatory Hill Formation (Marla Group). Geological Province: Officer Basin.||||||10-AUG-07
34977|Cadney Park Member|69445|5|Briefly described|p30:6|Early Cambrian|Early Cambrian|Extreme east of the Officer Basin.|||||Includes basaltic rocks and tuffs.|12-JUL-16
34977|Cadney Park Member|72478|6|Mentioned|p8|Early Cambrian|Early Cambrian|Officer Basin. See also Cadney Park Formation p51 [of the document].||Observatory Hill Formation||||29-MAR-21
34977|Cadney Park Member|73099|5|Briefly described|Map legend.|Middle Cambrian|Early Cambrian|Officer Basin.||Basal Observatory Hill Formation.||Overlies Relief Sandstone. Is overlain by Parakeelya Alkali Member.|Grey, brown and red-brown siltstone and claystone, micaceous and dolomitic or calcareous in places, dolostone and limestone, very fine- to very coarse-grained sandstone; veins of gypsum, anhydrite and calcite.|
31781|Callamurra Member|13497|4|Described|iv, vi, viii, xii, p69 fig 6.1|Early Triassic|Late Permian|Cooper Basin. Informally defined by Channon and Wood (1989). A reference section was assigned by Channon and Wood (1989). Maximum drilled thickness of 150m in Moomba Field. Deposited in a fluvial floodplain environment. Regarded as a regional oil and gas seal unit. Hosts economic oil and gas reservoirs in places. Seal and reservoir characteristics discussed. See also p104-p110, p157 tbl 10.1, p159, p161, p165, p166 fig 10.8.||Arrabury Formation||Conformably overlies the Toolachee Formation. Disconformably overlain by the Paning Member. Overlain by the Wimma Sandstone Member.|Siltstone and mudstone beds with minor sandstone interbeds.|
31781|Callamurra Member|13516|5|Briefly described|p171 fig 12|Early Triassic||In Eromanga Basin.||Of Arrabury Formation||||
31781|Callamurra Member|22883|6|Mentioned|P29|||Parent is Arrabury Formation||||||
31781|Callamurra Member|23155|6|Mentioned|Fig 8 on p16|Triassic|Permian|||||||
31781|Callamurra Member|23375|4|Described|Fig2 p265,280|Dorashamian|Dzhulfian|Of the Arrabury Formation.Geological Province: Cooper Basin.||||||30-JUN-08
31781|Callamurra Member|24210|5|Briefly described|p133 Fig. 2|Early Triassic|Late Permian|Of the Arrabury Formation (Nappamerri Group).  Geological Province: Cooper Basin.||||||
31781|Callamurra Member|44133|5|Briefly described|p65 Fig. 8.3, 85|Triassic|Permain|Of the Arrabury Formation. Geological Province: Cooper Basin. ||||||
31781|Callamurra Member|60717|5|Briefly described|p40 Fig. 2|Scythian|Tatarian|Of Arrabury Formation (Nappamerri Group). Overlies Toolachee Formation; overlain by other members of the unit - Paning and Wimma Sandstone Members.  Thickness: 125m. Geological Province: Cooper Basin.||||||31-JAN-08
31781|Callamurra Member|61015|6|Mentioned|p44|||Of the Birkhead Formation?  Contains gas.||||||19-APR-05
31781|Callamurra Member|61613|5|Briefly described|p282 Fig. 2|Late Permian|Late Permian|Of Arrabury Formation. Overlain by Paning Member. Geological Province: Cooper and Simpson Basins.||||||07-FEB-11
31781|Callamurra Member|61616|6|Mentioned|p330 Fig. 2|Early Triassic|Late Permian|Of Arrabury Formation. Geological Province: Cooper Basin.||||||31-MAR-09
31781|Callamurra Member|62537|6|Mentioned|p191 Fig.2. |Early Triassic|Early Triassic|Cooper Basin.||Unit in Arrabury Formation.||||
31781|Callamurra Member|62730|5|Briefly described|p352 Fig. 1|Early Triassic|Late Permian|Of the Arrabury Formation. Geological Province: Cooper Basin.||||||21-APR-08
31781|Callamurra Member|63978|2|Defined|p7, p19-20, Fig. 3|Early Triassic|Late Permian|Basal member of Arrabury Fm (Nappamerri Gp). Conformable on Toolachee Fm; overlain by Paning Mbr (disconformably in places). Max.thickness: 170m. In Cooper Basin. Lower carbonaceous mudst.+ siltst., overlain by interbedded mudst.+ siltst.+ lesser sst.||||||07-FEB-11
31781|Callamurra Member|64048|5|Briefly described|p67|||Within the lower Arrabury Formation. Contains a sandstone gas reservoir ~10m thick. Dominantly sandstone and mudstone - interbedded siltstones, mudstones and very fine-grained sandstones.||||||07-FEB-11
31781|Callamurra Member|64197|6|Mentioned|p625 Fig.1c|Early Triassic|Late Permian|Cooper Basin.||||Underlies the Paning Member; overlies the Toolachee Formation.||
31781|Callamurra Member|64665|5|Briefly described|p53 Fig.2.|Early Triassic|Early Triassic|Cooper Basin.||Basal unit in Arrabury Formation.||||
31781|Callamurra Member|65489|5|Briefly described|p48, p96, p131-132|Scythian|Tatarian|125m thick. Regarded as a regional seal; also contains economic oil and gas reservoirs locally, and is a leaky seal elsewhere.||Basal unit in Arrabury Formation.||Overlies Toolachee Formation (Gidgealpa Group). Is overlain by Paning and Wimma Sandstone Members.||
31781|Callamurra Member|67402|5|Briefly described|p90 fig CPR4, p91 tbl CPR1|||Deposited in floodplain and shallow perennial lacustrine environments. Maximum thickness of 170m. See also p90-p94, p98, p100, p101 tbl CPR2, p103, p303.||Arrabury Formation||Conformably overlies the Toolachee Formation. Conformably overlain by the Paning Member.|Mudstone and siltstone sequence with minor fine to medium-grained sandstone interbeds.|
31781|Callamurra Member|68731|5|Briefly described|p200 Fig 3.110, p207|Early Triassic|Lopingian|Also mis-spelt as the Calamurra Member on p207. Includes rocks assigned to the lower Paning Member by Powis (1989). Flood plains and shallow perennial lakes, with input from meandering streams. Includes late Lopingian-early Triassic palynofloras.||Of the Arrabury Formation.||Conformably underlain by the Toolachee Formation. Unconformably underlain by the Innamincka Formation. Overlain by the Paning Member (possible disconformity).|Carbonaceous mudstone and siltstone, which grade up into organically lean, partly mottled mudstone and siltstone, with lesser fine to medium, moderately sorted quartzose, in part micaceous sandstone with an argillaceous and siliceous matrix.|02-JUL-14
31781|Callamurra Member|69797|5|Briefly described|p17 Fig.2|Early Triassic|Late Permian|Age: Tatarian - Scythian (approximated from figure). Geol. Prov: Cooper Basin.||Arrabury Formation||||
31781|Callamurra Member|69946|5|Briefly described|p9, p36, p54|Early Triassic|Permian|Cooper Basin.||Unit in Arrabury Formation.||Overlies Toolachee Formation. Is overlain by Paning Member.||
31781|Callamurra Member|69947|5|Briefly described|p13 Fig.7.2|Early Triassic|Permian|Cooper Basin.||Arrabury Formation.||||
31781|Callamurra Member|70317|6|Mentioned|p33|Early Triassic|Late Permian|Cooper Basin.||Arrabury Formation.||Overlies Toolachee Formation. Is overlain by Paning, and Wimma Sandstone, Members.||
31781|Callamurra Member|70823|5|Briefly described|p40, p75, p79, p81, p82|||Cooper Basin. Contains economic oil and gas reservoirs locally.||Arrabury Formation||Overlain by the Wimma Sandstone Member.|Thin fine to medium grained quartzose sandstones.|
31781|Callamurra Member|70824|4|Described|p7, p104|Induan|Induan|Cooper Basin. Deposited in floodplains, lacustrine environments and moderate sinuosity fluvial environments.||Arrabury Formation||Overlies the Toolachee Formation. Unconformably overlain by the Paning Member.|Basal mudstone and siltstone with thin fine to medium-grained quartzose sandstone interbeds.|
31781|Callamurra Member|70946|5|Briefly described|p1089|Early Triassic|Permian|Cooper Basin. Deposited in a floodplain, lacustrine or moderate sinuosity fluvial channel environment.||Arrabury Formation.||Unconformably overlain by Paning Member.||08-OCT-18
31781|Callamurra Member|71265|5|Briefly described|p589|Induan|Induan|Cooper Basin.||Arrabury Formation.||Overlies Toolachee Formation. Is overlain by Paning Member.||
31781|Callamurra Member|71342|6|Mentioned|Ch5 p9, Ch5 p54, Ch7 p13|Scythian|Tatarian|Cooper Basin. Palynological zone is given in fig 5.3 Ch5 p36. Deposited in floodplain, lacustrine or fluvial channel environments.||Arrabury Formation||Overlies the Toolachee Formation. Overlain by the Paning Member.||
31781|Callamurra Member|71701|5|Briefly described|p155|Olenekian|Induan|Cooper Basin.||Arrabury Formation||Unconformably overlain by the Paning Member.||
31781|Callamurra Member|72297|5|Briefly described|p742|||Cooper Basin; absent in the E and N areas. Acts as a regional seal.||Basal Arrabury Formation.||||
31781|Callamurra Member|73167|6|Mentioned|p664 Fig. 2|Triassic|Triassic|Cooper Basin. Contains gas.||Nappamerri Group||||
31781|Callamurra Member|73244|6|Mentioned|p86|Triassic|Triassic|Cooper Basin.  Along with Panning Member, Wimma Sandstone Member and Tinchoo Formation, shown as floodplain, lacustrine, fluvial channels. Gas.||||||
31781|Callamurra Member|73251|6|Mentioned|p62|Early Triassic|Permian|Cooper Basin. Lacustrine and moderately sinuous fluvial channel depositional environments. Contains[?] gas.||Arrabury Formation, Nappamerri Group||Underlain by Toolachee Formation (Gidgealpa Group). Overlain by Arrabury Formation including Callamurra Member.||
31781|Callamurra Member|73343|6|Mentioned|p337|Triassic|Triassic|Cooper Basin. Hosts gas.||Nappamerri Group||Underlain by Toolachee Formation. Overlain by Panning Member.||
31781|Callamurra Member|73479|5|Briefly described|p156 Fig.2, p159|Triassic|Triassic|Cooper Basin. Floodplain, lacustrine, fluvial channels depositional environment.|ca 245 Ma|Nappamerri Group||Overlies Toolachee Formation, underlies Panning Member||
24206|Calthorinna Tillite|22510|5|Briefly described|p38,41|||Of the Yudnamutana Subgroup.  Peake and Denison Inliers.||||||13-OCT-04
24206|Calthorinna Tillite|23054|5|Briefly described|p14-5|||||||||
24206|Calthorinna Tillite|23282|6|Mentioned|p55|||of Peake and Denison Inlier and equivalent to Chambers Bluff Tillite.||||||
24206|Calthorinna Tillite|36733|2|Defined|p71|Adelaidean|Adelaidean|See also P47.||||||
24206|Calthorinna Tillite|37932|5|Briefly described|p541|||||||||
24206|Calthorinna Tillite|38108|6|Mentioned|Table 1|||||||||
24206|Calthorinna Tillite|39344|6|Mentioned|Map legend|Precambrian|Precambrian|Sturtian||||||
24206|Calthorinna Tillite|41405|3|Fully described|p154|||||||||
24206|Calthorinna Tillite|42222|6|Mentioned|p16|||||||||
24206|Calthorinna Tillite|43052|5|Briefly described|p183,Table 6.2|||||||||
24206|Calthorinna Tillite|44289|5|Briefly described|Map Legend||Proterozoic|||||||
24206|Calthorinna Tillite|65365|6|Mentioned|p9 Fig. 3|||Peake and Denison Ranges, northern Adelaide Rift Complex.||||||19-MAR-12
75787|Camel Flat Shale Member|66884|1|Redefined|p38, p39 Fig.2, p41 Fig.3, p44|||Resurrected name (previously used as Camel Flat Shale in unpubl. thesis by Murrell, 1977). Lowermost unit in Skillogalee Dolomite. Indicates transgression prior to onset of carbonate sedimentation of Skillogalee Dolomite. Deposition in lagoonal environment (Belperio 1987; Forbes 1990) marks change from underlying sand-dominated units to dolomite-rich units above. Thickness: ~200 m near Mount Norwest Gorge; ~120 m in type section. Type locality in eastern Willouran Ranges consists of outcrops directly south of dirt track between Witchelina diapir and Old Mount North West Homestead (29o56.839'S, 138o4.676'E to 29o56.772'S, 138o4.352'E). Age: Mid Torrensian. Shortened to Camel Flat Shale on p38.||Skillogalee Dolomite||Conformably overlies Witchelina Quartzite (Emeroo Subgroup); is conformably overlain by Twenty Mile Hill Member.|Black pyritic shale with interbedded dolomite lenses; dark grey to green, laminated shale interbedded with subordinate dolostone and quartz arenite overlying basal conglomerate lag.|14-DEC-16
29893|Camel Pad Granite|22631|6|Mentioned|p176|Calymmian|Calymmian|||||||
29893|Camel Pad Granite|24197|5|Briefly described|p75 Tb. 8.1|Mesoproterozoic|Mesoproterozoic|Age: 1560Ma.||||||07-FEB-11
29893|Camel Pad Granite|43052|5|Briefly described|Table 4.8|||||||||
29893|Camel Pad Granite|50605|5|Briefly described|p(ii), 1.4, 10.2, Table 1.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Gawler Craton & Curnamona Province. Of the Moolawatana Suite. Age: ~1560Ma.||||||
29893|Camel Pad Granite|66302|6|Mentioned|p50|Calymmian|Calymmian|Moolawatana Domain, Curnamona Province.|1551 +/- 15 Ma (Fanning et al, 1998)|Moolawatana Suite||||
29893|Camel Pad Granite|70384|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic||1555 +/- 12 Ma (SHRIMP U-Pb zircon).||||Granite, fine-grained, with aggregates of biotite, and magnetite.|
29893|Camel Pad Granite|72459|6|Mentioned|p67|||Represents, alongside other small granite bodies like the Old Camp Granite, the only known outcrop of 1555-1560 Ma Moolawatana magmatism in the SE Mt Painter Inlier.|1555-1560 Ma|Moolawatana Suite||||
36756|Cape Donnington Quartz Gabbro Norite Gneiss|23775|5|Briefly described|p724|Orosirian|Orosirian|Age: 1850 +/- 2 Ma, 1848.7 +/- 4.3 Ma, 1849.8 +/- 1.1 Ma||||||22-SEP-09
34794|Cape Willoughby Granite|9124|5|Briefly described|Map Legend|Paleozoic|Paleozoic|Porphyritic, coarse-grained adamellite.||||||11-JAN-10
34794|Cape Willoughby Granite|22766|5|Briefly described|Fig.2 p561|Middle Cambrian|Early Cambrian|Age of unit 508+/-7 Ma. See also Fig.1 p560||||||
34794|Cape Willoughby Granite|23317|6|Mentioned|p387|Middle Cambrian|Middle Cambrian|Age: 508+/-7Ma.  On Kangaroo Isalnd.||||||07-FEB-07
34794|Cape Willoughby Granite|23996|6|Mentioned|p352|||Geological Province: Adelaid Fold Belt.||||||07-MAR-05
34794|Cape Willoughby Granite|44133|5|Briefly described|p56 Table 7.3|Ordovician|Cambrian|I-Type. Megacrystic granite. Age: 472-475Ma, 508 +/- 7Ma.||||||
34794|Cape Willoughby Granite|61307|5|Briefly described|p14 Fig. 6|Middle Cambrian|Early Cambrian|Age: 508+/-7Ma. ||||||
34794|Cape Willoughby Granite|64282|5|Briefly described|Map legend|Middle Cambrian|Middle Cambrian|Age: 508+/-7Ma (U-Pb). Part of Delamerian Orogeny. Coarse-gr., equigranular granite with quartz, microcline and plagioclase, and minor biotite; opalescent blue quartz is present as is magmatic layering and xenoliths of the Kanmantoo Group metasandstone.||||||23-JUN-08
34794|Cape Willoughby Granite|65921|5|Briefly described|p1|||Occurs at Cape Willoughby. Contains inclusions of Kanmantoo Group sediments.|c.508 Ma.||||Coarse grained granite. Preserved magma layering is visible in outcrop along with inclusions of Kanmantoo Group sediments with retained bedding.|
34794|Cape Willoughby Granite|73107|5|Briefly described|Map legend.|Middle Cambrian|Middle Cambrian|Delamerian Orogeny.|508 +/- 7 Ma.||||Coarse-grained equigranular granite with quartz, microcline and plagioclase and minor biotite. Opalescent blue quartz is present, as is magmatic layering and xenoliths of Kanmantoo Group metasandstone.|
34285|Carcase Rock Granite|22690|6|Mentioned|p306||Orosirian|Alkali- feldspar granite.||Donington Granitoid Suite.||||23-AUG-18
34285|Carcase Rock Granite|73525|5|Briefly described|p19 Fig.13|||Spencer Domain.||Donington Suite|||Felsic intrusive.|
34656|Carey Gully Sandstone Member|22869|2|Defined|P38, P45||Neoproterozoic|New name, correlated to the River Wakefield Subgroup and Bungaree Quartzite, parent is Aldgate Sandstone||||||
34656|Carey Gully Sandstone Member|22889|6|Mentioned|Table 1 on p32|Adelaidean|Adelaidean|Parent - Aldgate Sandstone of the Emeroo Subgroup.||||||
23472|Carnding Rhyodacite|39802|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
23472|Carnding Rhyodacite|40644|6|Mentioned|p124 Fig. 3, p135 Tb. 4|Mesoproterozoic||Age: 1501+/-123Ma.||||||02-JUN-09
23472|Carnding Rhyodacite|41972|6|Mentioned|Table 3 p378|||||||||19-JUN-19
23472|Carnding Rhyodacite|42469|6|Mentioned|p16|||Map sheet: Tarcoola, SH53-10.||||||02-JUN-09
23472|Carnding Rhyodacite|42546|5|Briefly described|Map legend|Mesoproterozoic||||||||
23472|Carnding Rhyodacite|42736|5|Briefly described|map legend|Mesoproterozoic||||||||
23472|Carnding Rhyodacite|43052|5|Briefly described|p117|||Of Gawler Range Volcanics.||||||02-JUN-09
23472|Carnding Rhyodacite|44935|5|Briefly described|Map Legend||Proterozoic|||||||
23472|Carnding Rhyodacite|68131|6|Mentioned|p77|Mesoproterozoic|Mesoproterozoic|||||||
23472|Carnding Rhyodacite|70659|5|Briefly described|p6 fig 2, p8|Mesoproterozoic|Mesoproterozoic|Tarcoola-Kingoonya area.||Upper Gawler Range Volcanics.|||Rhyodacite.|
23472|Carnding Rhyodacite|70816|5|Briefly described|p5|||Tarcoola-Kingoonya area, Gawler Ranges.||Unit of upper Gawler Range Volcanics.||Equivalent to Chandabooka Dacite and Yardea Dacite.||
23472|Carnding Rhyodacite|72090|6|Mentioned|p12|||Gawler Craton.||Gawler Range Volcanics, Upper||||
28206|Carnot Gneiss|22796|5|Briefly described|p76|||||||||
28206|Carnot Gneiss|24526|5|Briefly described|p95, p96 Fig. 2|Archean|Archean|Of the Sleaford Complex. Dominated by garnet-biotite-cordierite metapelite with lenses of mafic granulite, felsic augen gneiss and hypersthene-garnet gneiss. Geological Province: Gawler Craton.  See also p98 Fig. 4.||||||07-NOV-08
28206|Carnot Gneiss|40448|5|Briefly described|p27|||||||||27-JAN-17
28206|Carnot Gneiss|50130|6|Mentioned|p6|||Geological Province: Gawler Craton.||||||
28206|Carnot Gneiss|50605|5|Briefly described|p4.2|||Of the Sleaford Complex. Geological Province: Gawler Craton & Curnamona Province.||||||
28206|Carnot Gneiss|64131|5|Briefly described|p1401|||||Of the Sleaford Complex.|||Paragneiss and orthogneiss.|
28206|Carnot Gneiss|64722|5|Briefly described|p12||Neoarchean|Contains 3150-2950 and 2850-2500 Ma detrital zircons.||||||
28206|Carnot Gneiss|65915|5|Briefly described|p18|Siderian|Siderian|Of Sleaford Complex. ~2450 Ma.||||||
28206|Carnot Gneiss|66302|5|Briefly described|p10, p11, p13, p25, p61, p61 Fig.14|||Protolith interpreted to have been deposited between 2535 and 2500 Ma in an extensional back arc setting.||Sleaford Complex|||Garnet quartz-feldspar paragneiss, augen gneiss and garnet gneiss with boudins of mafic granulite interpeted to be derived from tholeiitic basalt or gabbro sills prior to metamorphism.|
28206|Carnot Gneiss|67058|5|Briefly described|p476, p492.|Neoarchean|Neoarchean|Southern Gawler Craton.|c.2520 Ma.|Unit in Sleaford Complex.||||15-MAR-12
28206|Carnot Gneiss|68131|6|Mentioned|p66|Paleoproterozoic|Archean|Coffin Bay Peninsula.||||||
28206|Carnot Gneiss|69048|5|Briefly described|p4, p13-23, p29-36, p67|||SHRIMP U-Pb detrital zircon ages from Redbanks and Cape Carnot. Two ages of metamorphism were also determined: 2465 +/- 8 Ma (Sleafordian Orogeny) and 1726 +/- 24 Ma (Kimban Orogeny). The granite gneiss magmatic crystallisation age was determined at 2431 +/- 7 Ma; migmatite-grade metamorphism at 1715 +/- 6 Ma.|2514 +/- 7 Ma (maximum depositional age).||||Garnetiferous metasedimentary rock; garnet-bearing quartzo-feldspathic gneiss. Compositionally layered with biotite-rich, cordierite-rich and garnet-rich zones. Also includes a migmatitic, K-feldspar megacrystic, garnetiferous granite gneiss.|25-JAN-17
28206|Carnot Gneiss|71859|4|Described|p2, p6-p8, p14, p28, p36|Neoarchean|Neoarchean|Southern Gawler Craton. Exposed in coastal sections between Sleaford Bay and Cape Carnot on the Southern Eyre Peninsula. MDA of paragneiss is also derived from Jagodzinski et al., 2012. Mineralogy of paragneiss and orthogneiss discussed. Subjected to granulite facies metamorphism during the Sleafordian Orogeny.|2540 +/- 45 to 2514 +/- 7 Ma (Lane, 2011)|Sleaford Complex|||Composite geological unit of felsic orthogneiss, metabasalt, granite and siliciclastic paragneiss.|04-APR-23
28206|Carnot Gneiss|73026|4|Described|p24-25|Siderian|Siderian|The type locality occurs immediately west of the headland at Cape Carnot. SHRIMP ages include peaks at 2431 +/- 7 Ma and 2481 +/- 8 Ma with numerous lesser age groups and a metamorphic age of 1715 +/- 6 Ma. It is unknown wheter 2431 or 2481 represent the magmatic ages or not. This unit has an inferred S-type affinity. Associated with the Sleafordian event.|||||Granitic gneiss, metapelite and deformed mafic dykes.|
28206|Carnot Gneiss|73027|4|Described|p29-30, p32, p35, p41|Siderian|Siderian|Dips steeply east in Red Banks and contains a strong folation with asymmetric fabric elements. The type locality for the unit is Cape Carnot. Metamorphic ages are dated at 1715 +/- 6 Ma (SHRIMP U-Pb). Abundant garnet and cordierite suggest the granite gneiss has an S-type affinity with an inherited zircon component. It is unclear whether 2481+/- 8 ma is the magmatic age or if the 2431 age is the magmatic age and the former is inherited.|2481 +/- 8 ma to 2431 +/- 7 (SHRIMP U-Pb)|||Intruded by the Red Banks Charnockite.|Granitic gneiss, metapelite, deformed mafic dykes and migmatitic garnet-sillimanite-biotite-cordierite-bearing assemblages.|
24213|Carnot Gneisses|22629|6|Mentioned|p145|||||||||
24213|Carnot Gneisses|23491|6|Mentioned|p17|||Geological Province: Sleaford Complex.||||||
24213|Carnot Gneisses|23719|5|Briefly described|p20|Paleoproterozoic|Paleoproterozoic|Of Sleaford Complex. Geological Province: Gawler Craton.||||||07-NOV-08
24213|Carnot Gneisses|23791|5|Briefly described|p2|Archean|Archean|Part of the Sleaford Complex. Geological Province: Gawler Craton.||||||02-JUN-09
24213|Carnot Gneisses|24508|5|Briefly described|p30|||Age: ~2000Ma. Juxtapositioned with upper crustal Dutton Suite. Geological Province: Gawler Craton.||||||27-MAY-08
24213|Carnot Gneisses|24525|6|Mentioned|p207|Archean|Archean|Age: 3050-3150Ma.||||||07-NOV-08
24213|Carnot Gneisses|37620|2|Defined|p8|Paleoproterozoic|Neoarchean|Late Archaean/Early Proterozoic age.||||||07-NOV-08
24213|Carnot Gneisses|37811|6|Mentioned|Fig.3|||||||||
24213|Carnot Gneisses|39010|5|Briefly described|p68|||||||||
24213|Carnot Gneisses|39802|6|Mentioned|Map legend|Archean|Archean|||||||
24213|Carnot Gneisses|40448|5|Briefly described|p23-27|Archean|Archean|Fanning et al. (1981). Southern Eyre Peninsula.|2586+/-131 Ma - 2412+/- 72 Ma|Sleaford Complex.||Wangary Gneisses may be less-metamorphosed equivalent.|An extensive layered sequence mainly of thinly layered, garnetiferous quartzofeldspathic gneisses, often intercalated with leucogneiss, biotite-garnet gneiss, felsic gneiss and basic granulite.|
24213|Carnot Gneisses|40644|6|Mentioned|p120, p126|Paleoproterozoic|Archean|Of Fanning et al (1981). [Superseded by Carnot Gneiss?]. Age: >2500Ma. Included in the Sleaford Complex grouping.||||||25-JAN-17
24213|Carnot Gneisses|41667|5|Briefly described|p2|||||||||
24213|Carnot Gneisses|41972|6|Mentioned|Fig.3 p366|Archean|Archean|||||||
24213|Carnot Gneisses|42468|5|Briefly described|p13|Neoarchean|Neoarchean|Of Sleaford Complex, Gawler Craton. Southern Eyre Peninsula.||||||
24213|Carnot Gneisses|42934|5|Briefly described|p524|||||||||
24213|Carnot Gneisses|43052|4|Described|p33,Table 3.1|||Of Sleaford Complex.||||||27-MAY-08
24213|Carnot Gneisses|60534|5|Briefly described|p572|Archean|Archean|Of the Sleaford Complex. Geological Province: Gawler Craton.||||||
24213|Carnot Gneisses|61070|5|Briefly described|Map Legend|Proterozoic|Archean|Of the Sleaford Complex. Undifferentiated interlayered para-orthogneisses, plus mafic granulites. Age: 2637 +/- 21Ma ; ~2440 Ma (U-Pb Zircon, age of metamorphism. Sm-Nd isotopes suggest age of ~3000-2700Ma for source). Geological Province: Gawler Craton.||||||12-JAN-10
24213|Carnot Gneisses|61307|5|Briefly described|p35|Archean|Archean|Part of the Sleaford Complex.  Age: >2600Ma. Geological Province: Gawler Craton.||||||07-NOV-08
24213|Carnot Gneisses|61725|5|Briefly described|p893|Archean|Archean|Of the Sleaford Complex. Crystalline with low primary porosity.||||||07-NOV-08
24213|Carnot Gneisses|64828|5|Briefly described|p1065 Fig. 2|Paleoproterozoic|Archean|Probably should be Carnot Gneiss? Included in the Sleaford Complex.||||||04-MAR-09
24213|Carnot Gneisses|65376|6|Mentioned|p15, 21,33, 34, 45,60.|||[Superseded by Carnot Gneiss?]. Crops out along western Sleaford Bay.||Unit in Sleaford Complex.|||Garnetiferous.|25-JAN-17
24213|Carnot Gneisses|65390|5|Briefly described|p20|Orosirian|Orosirian|Gawler Craton. Zircon crystallisation recorded in this unit at c. 2000 Ma. Faulted against Dutton Suite.||||||
24213|Carnot Gneisses|65485|4|Described|p41-45|Archean|Archean|EPMA monazite geochronological results show that this unit was highly deformed and metamorphosed to granulite facies during the Kimban Orogeny (1708-1690 Ma), not the Sleafordian Orogeny (2450-2420 Ma).||Of the Sleaford Complex.|||Migmatitic garnet+cordierite+opx paragneiss; augen and charnockitic orthogneiss; garnet+CPX+OPX mafic granulites.|20-MAR-15
24213|Carnot Gneisses|65922|5|Briefly described|p9, 12, 14|Neoarchean|Neoarchean|Garnet gneiss, southern Eyre Peninsula, SA. Also recognised as extending north to the Kyancutta - Warramboo area. Probably equivalent to garnet gneiss within Sleaford Complex. Age ~2600 - 2500 Ma.||||||20-MAR-15
24213|Carnot Gneisses|68208|6|Mentioned|p31 Fig.2|||||Of Sleaford Complex||||
24213|Carnot Gneisses|73256|6|Mentioned|p559|||||Sleaford Complex|||Medium- to high-grade metamorphics.|
39862|Caroline Intrusive Complex|24496|5|Briefly described|p1, 65|Mesoproterozoic|Mesoproterozoic|Of Giles Complex. Contains layered sequences.  Geological Province: Musgrave Block.||||||04-FEB-05
39862|Caroline Intrusive Complex|24497|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Geological Province: Musgrave Block.||||||
39862|Caroline Intrusive Complex|24499|5|Briefly described|Map legend|||||||||
39862|Caroline Intrusive Complex|60660|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Geological Province: Musgrave Block.||||||22-FEB-05
39862|Caroline Intrusive Complex|60662|6|Mentioned|Map Legend|||Of Giles Complex.||||||22-FEB-05
29768|Caroona Siltstone Member|22510|5|Briefly described|table1p37|||Age: Marinoan. mid-North Region||||||
25836|Carrickalinga Head Formation|22573|6|Mentioned|p 53|||||||||
25836|Carrickalinga Head Formation|22581|5|Briefly described|Fig.2,p37|||Kanmantoo Group, Kanmantoo Basin. Overlies Truro Volcanics. Overlain by Backstairs Passage Formation||||||
25836|Carrickalinga Head Formation|22643|5|Briefly described|p188, fig3,6,7|Early Cambrian|Early Cambrian|||||||
25836|Carrickalinga Head Formation|22840|6|Mentioned|Table1 p38, p38|||||||||03-NOV-22
25836|Carrickalinga Head Formation|23317|5|Briefly described|380 Fig.2|||||||||
25836|Carrickalinga Head Formation|23539|4|Described|Fig 1 p 467|||Also see p 467- 469||||||
25836|Carrickalinga Head Formation|23818|5|Briefly described|p87 Fig.33|Cambrian|Cambrian|||||||
25836|Carrickalinga Head Formation|23981|5|Briefly described|p10 Fig. 5, p26|Toyonian|Early Cambrian|Of Kanmantoo Group. Olive-green lithic sst. with thin shale interbeds; fining upwards to thin siltstones. Has significantly eroded Heatherdale Shale below in some areas. Overlain by remainder of Kanmantoo Gp. siliciclastic metseds. In Stansbury Basin.||||||04-FEB-08
25836|Carrickalinga Head Formation|23996|5|Briefly described|p352 Fig.1|Cambrian|Cambrian|Of Kanmantoo Group.  Geological Province: Adelaid Fold Belt.||||||07-MAR-05
25836|Carrickalinga Head Formation|24361|6|Mentioned|p50, p50 Fig.1b|||Of the Kanmantoo Group.||||||
25836|Carrickalinga Head Formation|24465|4|Described|p347|Early Cambrian|Early Cambrian|Basal unit of the Kanmantoo Group.||||||
25836|Carrickalinga Head Formation|30052|6|Mentioned|Fig.3|||Cambrian age.||||||
25836|Carrickalinga Head Formation|30377|2|Defined|p203|Early Cambrian|Early Cambrian|See also p204. Member of Kanmantoo Group||||||26-JUN-08
25836|Carrickalinga Head Formation|30378|6|Mentioned|p432|||||||||
25836|Carrickalinga Head Formation|30379|5|Briefly described|p89|||Lower Cambrian age.Includes Madigan Inlet member.||||||
25836|Carrickalinga Head Formation|30380|6|Mentioned|Table 1|||Correlation||||||
25836|Carrickalinga Head Formation|30381|6|Mentioned|Fig.4|||||||||
25836|Carrickalinga Head Formation|30801|6|Mentioned|p5|||Kanmantoo Group. Table P5-6. Equivalent? to Strangway Hill Fornation||||||
25836|Carrickalinga Head Formation|33471|6|Mentioned|p555|||||||||
25836|Carrickalinga Head Formation|33953|6|Mentioned|Fig.4|||||||||
25836|Carrickalinga Head Formation|34014|5|Briefly described|p23|||Camb.||||||
25836|Carrickalinga Head Formation|34612|6|Mentioned|Fig.33|||Correlation chart. Cambrian||||||
25836|Carrickalinga Head Formation|35255|6|Mentioned|Fig.8|||||||||
25836|Carrickalinga Head Formation|36198|6|Mentioned|Fig.I.2|||||||||
25836|Carrickalinga Head Formation|36731|6|Mentioned|p125|||||||||
25836|Carrickalinga Head Formation|36836|6|Mentioned|Table 1|||||||||
25836|Carrickalinga Head Formation|38873|4|Described|Table 2|||||||||
25836|Carrickalinga Head Formation|39350|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
25836|Carrickalinga Head Formation|39806|6|Mentioned|p207|||||||||
25836|Carrickalinga Head Formation|40228|5|Briefly described|p39|||||||||
25836|Carrickalinga Head Formation|40442|6|Mentioned|p16|||||||||
25836|Carrickalinga Head Formation|40454|6|Mentioned|p46|||||||||
25836|Carrickalinga Head Formation|40455|5|Briefly described|p71|||||||||
25836|Carrickalinga Head Formation|40856|6|Mentioned|Fig.23.6|||||||||
25836|Carrickalinga Head Formation|41853|6|Mentioned|p199|||||||||
25836|Carrickalinga Head Formation|41947|5|Briefly described|p16|||||||||
25836|Carrickalinga Head Formation|42101|6|Mentioned|p84|||||||||
25836|Carrickalinga Head Formation|42222|6|Mentioned|Table 1 p4|||||||||03-NOV-22
25836|Carrickalinga Head Formation|42225|6|Mentioned|Fig.4 p224|||||||||03-NOV-22
25836|Carrickalinga Head Formation|42243|5|Briefly described|p211|||||||||
25836|Carrickalinga Head Formation|42266|5|Briefly described|p291|||||||||
25836|Carrickalinga Head Formation|42269|5|Briefly described|p336|||||||||
25836|Carrickalinga Head Formation|42270|4|Described|p352|||||||||
25836|Carrickalinga Head Formation|42271|6|Mentioned|p378|||||||||
25836|Carrickalinga Head Formation|42272|5|Briefly described|p404|||||||||
25836|Carrickalinga Head Formation|42488|5|Briefly described|p191, Fig.2 p187|||||||||
25836|Carrickalinga Head Formation|42499|5|Briefly described|Map legend|Cambrian||||||||
25836|Carrickalinga Head Formation|42505|5|Briefly described|Map legend|Cambrian||||||||
25836|Carrickalinga Head Formation|43052|5|Briefly described|Table 2.1|||||||||
25836|Carrickalinga Head Formation|43190|5|Briefly described|p34.|||Of Kanmantoo Group.||||||
25836|Carrickalinga Head Formation|43192|6|Mentioned|p63|||Of Kanmantoo Group.||||||27-MAY-08
25836|Carrickalinga Head Formation|43703|6|Mentioned|p75|||||||||
25836|Carrickalinga Head Formation|43759|6|Mentioned|p445|||||||||
25836|Carrickalinga Head Formation|44133|5|Briefly described|p4 Fig. 7.2, 6, 7 Fig. 7.4|Early Cambrian|Early Cambrian|Geological Province: Stansbury Basin. Of the Kanmantoo Group. Includes: Campana Creek Member, Blowhole Creek Siltstone, Madigan Inlet Member.||||||
25836|Carrickalinga Head Formation|50154|6|Mentioned|p200|||Consists of laminated phyllites, metasiltstones and metasandstones||||||
25836|Carrickalinga Head Formation|60712|5|Briefly described|p27, p28 Fig. 1|Early Cambrian|Early Cambrian|Of Daily and Milnes (1972, 1973).  Of the Kanmantoo Group.  See also p30 Fig. 3.||||||31-MAY-05
25836|Carrickalinga Head Formation|61046|5|Briefly described|p8 Fig. 2|Early Cambrian|Early Cambrian|Of Kanmantoo Group. Laminated metasiltstone, metasandstone, minor marble.||||||
25836|Carrickalinga Head Formation|61307|5|Briefly described|p6 Fig. 3|Cambrian|Cambrian|Of the Kanmantoo Group.  Includes marble units. Geological Province: Adelaide Fold Belt.||||||
25836|Carrickalinga Head Formation|63848|5|Briefly described|p531, p532, p534 Fig.4, p535, p537.|||||Unit in Kanmantoo Group.|Includes Madigan Inlet, Milendella, and Blowhole Creek Members.|Overlies Heatherdale Shale. Is overlain by Backstairs Passage Formation.||
25836|Carrickalinga Head Formation|64282|5|Briefly described|Map legend|Early Cambrian|Early Cambrian|Of the Kanmantoo Group. Geological Province: Kanmantoo Trough. Thick-bedded, grey metasandstone with thinly bedded muddy siltstone interbeds.||||||24-JUL-08
25836|Carrickalinga Head Formation|64746|6|Mentioned|p394. |||Contains detrital zircons aged 950-900 Ma.||Unit in Kanmantoo Group.||||
25836|Carrickalinga Head Formation|65375|5|Briefly described|p33.|Early Cambrian|Early Cambrian|||Unit in Kanmantoo Group.||Overlies Heatherdale Shale. Is overlain by Backstairs Passage Formation.||
25836|Carrickalinga Head Formation|65664|5|Briefly described|p1096, p1098, pp1100-4, p1106 Fig.5|Early Cambrian|Early Cambrian|Deposited in a deep water turbiditic environment.||Of Keynes Subgroup.||Unconformably overlies Normanville Group. Overlain by Backstairs Passage Formation.||09-MAY-12
25836|Carrickalinga Head Formation|65892|5|Briefly described|p9 Fig.4, p15-16, p19-20. |Middle Cambrian|Early Cambrian|Fleurieu Peninsula.||Basal unit in Kanmantoo Group.|Includes Madigan Inlet Member.|Disconformably overlies Heatherdale Shale and Truro Volcanics. Is overlain by Backstairs Passage Formation.||
25836|Carrickalinga Head Formation|65921|6|Mentioned|p1, p2 (map legend).|Cambrian|Cambrian|||Of the Kanmantoo Group.||||
25836|Carrickalinga Head Formation|66623|5|Briefly described|p430.|||||Basal unit of Kanmantoo Group.||Overlies Heatherdale Shale.|Dirty turbiditic sandstones.|
25836|Carrickalinga Head Formation|68735|5|Briefly described|p235 Fig.3|Early Cambrian|Early Cambrian|Fleurieu Peninsula.||Of the Kanmantoo Group.||||10-APR-17
25836|Carrickalinga Head Formation|68993|6|Mentioned|p544 Fig.1|Early Cambrian|Early Cambrian|Fleurieu Peninsula.||||||
25836|Carrickalinga Head Formation|69213|5|Briefly described|p37, 38|||Unmetamorphosed in Fleurieu Peninsula type area, but migmatised in eastern Mount Lofty Ranges. Extremely rapidly deposited and likely to have still contained significant pore fluids when buried to at least 10 km depth.||Basal unit of Kanmantoo Group.|||Dirty sandstone and siltstone alternating. Sillimanite-grade metamorphism and migmatisation found in eastern Mt Lofty Ranges. Migmatites range from metatexite to transitional diatexite. Coarse-grained biotite-rich schist also present.|
25836|Carrickalinga Head Formation|70382|6|Mentioned|p31 fig 6, p34|||Deformed and metamorphosed during Cambrian Delamarian Orogeny.||Unit of Kanmantoo Group.||Lowermost unit of Kanmantoo Group.||
25836|Carrickalinga Head Formation|73093|5|Briefly described|map legend|Cambrian|Cambrian||||||Sandstone, grey, with siltstone interbeds. Minor cross-bedding, ripples.|09-DEC-21
25836|Carrickalinga Head Formation|73107|5|Briefly described|Map legend.|Early Cambrian|Early Cambrian|Kanmantoo Trough.||Kanmantoo Group.|||Thick-bedded, grey metasandstone with thinly-bedded muddy siltstone interbeds.|
25836|Carrickalinga Head Formation|73188|5|Briefly described|p316, p353|Early Cambrian|Early Cambrian|Mount Lofty Ranges. Basal unit of the Kanmantoo Group.||Keynes Subgroup, Kanmantoo Group|||Turbidites, siltstone, limestone.|
25836|Carrickalinga Head Formation|73264|6|Mentioned|p1387 Fig.10|||||Kanmantoo Group||||
26464|Cartoberinna Granite|31698|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
26464|Cartoberinna Granite|35628|4|Described|Table 1|||Also P10||||||
26464|Cartoberinna Granite|50607|5|Briefly described|p2.2|||Geological Province: Musgrave Block. Of the Southern granites Suite (Kulgera Supersuite). Age range 1190-1150.||||||28-SEP-12
29922|Cartu beds|23288|6|Mentioned|Fig.5||Early Ordovician|||||||
29922|Cartu beds|23858|5|Briefly described|p917|Ordovician|Cambrian|Geological Province: Officer Basin.||||||
29922|Cartu beds|43052|5|Briefly described|Fig. 2.10|||||||||
29922|Cartu beds|44133|5|Briefly described|p40-41, 4 Fig. 7.2|Middle Paleozoic|Early Paleozoic|Geological Province: Eastern Officer Basin. Of the 'Munda Sequence'. Underlies Mintabie beds. Overlies: Blue Hills Sandstone ). ||||||07-NOV-08
26467|Castambul Formation|22869|5|Briefly described|P38, Fig2, Fig3, Fig||Neoproterozoic|Overlying unit is Basket Range Sandstone.||||||03-FEB-09
26467|Castambul Formation|22889|6|Mentioned|p34|Adelaidean|Adelaidean|Parent - Mundallio Subgroup.||||||
26467|Castambul Formation|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Torrensian||||||
26467|Castambul Formation|41404|4|Described|p98|||||||||
26467|Castambul Formation|42222|6|Mentioned|p14|||||||||
26467|Castambul Formation|42236|6|Mentioned|Fig.2 P106|||||||||
26467|Castambul Formation|43052|5|Briefly described|p179,Table 6.1|||Of Mundallio Subgroup.||||||03-FEB-09
26467|Castambul Formation|43190|6|Mentioned|p29|||See also Castambul Dolomite, Fig.2.||||||
26467|Castambul Formation|64647|5|Briefly described|p39 Fig. 2, p40|Neoproterozoic|Neoproterozoic|Of Burra Group. Knotted and pyritic schist, tremolitic dolomite marble, pink feldspathic quartzite.||||||
26467|Castambul Formation|73188|5|Briefly described|p316, p324, p327|Neoproterozoic|Neoproterozoic|Mount Lofty Ranges.||Mundallio Subgroup, Burra Group|||Pale dolomite, siltstone, quartzite.|
72577|Cathedral Rock Formation|62993|4|Described|p2, p3, p4, p8, p10, 12, 20, 39, 40, 43|Paleoproterozoic|Paleoproterozoic|Economically important unit as it is mineralised with Cu-Au-Ba. See also p16, p17, p20, p37.||Base of Ethiudna Subgroup||Unconformably overlies George Mine Formation|Volcanogenic quartzite at base, clast and matrix supported metamorphosed breccias with angular to subrounded, laminated albite rich clasts in a coarse grained matrix, dykes of granitic pegmatite and veins of calcalbitite.|19-DEC-21
72577|Cathedral Rock Formation|64741|5|Briefly described|p301 Fig. 4, p302|Paleoproterozoic|Paleoproterozoic|Of Ethiudna Subgroup (Curnamona Gp). Max.thickness: 100m. Geol.province: Olary Domain. Best developed over where the Ethiudna Subgroup overlies George Mine Formation. Varies from thin quartzite up to thick lenticular quartzite and pasmmopelitic units||||||07-FEB-11
72577|Cathedral Rock Formation|64944|5|Briefly described|p27, p28 Fig. 1, p29 Tb. 1|Paleoproterozoic|Paleoproterozoic|Of Ethiudna Subgroup (Curnamona Group). Age: <1718Ma. Includes quartzites which may have been deposited on a surface eroded into the Geroge Mine Formation; but absent or poorly developed above Tommie Wattie Formation. Locally volcaniclastic.||||||07-FEB-11
72577|Cathedral Rock Formation|66302|5|Briefly described|p36 Fig.9, p37, p39|Statherian|Statherian|Olary Domain, Curnamona Province. ||Ethiudna Subgroup||Overlain by the Peryhumuck Formation.|Quartz-rich metasedimentary and locally volcaniclastic rocks.|
72577|Cathedral Rock Formation|70339|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|||Ethiudna Subgroup.|||Quartzite, medium-grained, locally cross-bedded; minor iron-rich or volcaniclastic members.|27-JAN-16
72577|Cathedral Rock Formation|70405|4|Described|p2, p21,p22,p25,p26 plate 5,  |Paleoproterozoic|Paleoproterozoic|Barite-magnetite sedimentary exhalative formation.Yet to be formally defined (no type section yet described).Protoliths of feldspathic quartzose sandstone.Highly variable in thickness.||Ethiunda Subgroup||Overlies George Mine Formation, Underlies Peryhumuck Formation|Medium grained, Clean-variably feldspathic quartzitic metasediments. Psammopelitic to pelitic schists, quartzite, magnetite quartzite, quartz-pebble bearing quartzite and barite-magnetite and metacherts. Planar bedding to locally cross cross bedded.|
72577|Cathedral Rock Formation|70657|4|Described|p14-15, p18, p20-21, p23, p25-26, p28-30|Statherian|Statherian|A quartzite marker recognised by Campana and King (1958), Forbes (1991) and Conor (2000). The name Cathedral Rock Metasandstone Member was suggested by Zang (PIRSA, pers. comm., 2002); modified in this study to Cathedral Rock Formation. Curnamona Province; Olary Domain. No equivalent in Broken Hill Domain. Varying thickness (0 - 100m). Hosts the Mount Mulga Barite (Cu-Au) Mine.|<1718-1715 Ma|Basal Ethiudna Subgroup.||Overlies Mooleugore and George Mine Formations (Wiperaminga Subgroup). Underlies Peryhumuck and ?Bewooloo Formations.|Quartzite-bearing unit, locally volcaniclastic or magnetite-rich, occasionally baritic, and apparently preferentially developed above the George Mine Formation. Magnetite-rich; contains BIF.|
72577|Cathedral Rock Formation|70658|5|Briefly described|p3, 5-6, 8, 10, 12, 15-16, 18-19, 21, 25|Paleoproterozoic|Paleoproterozoic|See also p29, 41-47. Olary Domain, Curnamona Province. A very widespread regional marker. Hosts local quartz-barite-magnetite-sulphide units that are Cu-Au mineralised.||Ethiudna Subgroup.||Overlies Toraminga Formation and, unconformably, George Mine Formation.  Is overlain by Peryhumuck Formation.|Quartzite-dominated and psammopelite. Includes a Cu-Au-bearing quartz-magnetite-barite unit (exhalite) extending c.50km along strike (described in detail).|
23477|Cattlegrid Breccia|41405|6|Mentioned|p196|||||||||
23477|Cattlegrid Breccia|42168|5|Briefly described|p123|||||||||
68799|Chace Quartzite Member|60959|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Of the Rawnsley Quartzite. Mature, white, flat-bedded quartzite.||||||
68799|Chace Quartzite Member|61732|5|Briefly described|p28 Fig. 13|Marinoan|Marinoan|Of the Rawnsley Quartzite. Geological Province: Adelaide Rift Complex.||||||07-FEB-11
68799|Chace Quartzite Member|67484|6|Mentioned|p294 Tb.1|Ediacaran|Ediacaran|Adelaide Rift Complex.||Of Rawnsley Quartzite.||Overlain by Ediacara Member. Underlain by the Bonney Sandstone.||
68799|Chace Quartzite Member|67620|5|Briefly described|p5|Ediacaran|Ediacaran|Adelaide Rift Complex. Contains abundant elephant skin wrinkle structures (microbial mats).||Rawnsley Quartzite.||Overlies Bonney Sandstone. Is overlain by Ediacara Member.||
68799|Chace Quartzite Member|68030|3|Fully described|p239-241|Ediacaran|Ediacaran|Flinders Ranges.  Up to 250m thick and unfossiliferous. Petee laminations, featuring domed and disrupted, polygonal and sinuous ridges, overturning and roll-ups of sand are interpreted to be product of gas-doming and desiccation of microbial bound sand laminae on tidal flats (Gehling, 1999, 2000). Base of the Ediacaran Member represents a sequence boundary with 5-10m deep channels and regional 1-5km wide, 50-250m deep canyon incisions into Chace Quartzite Member, and locally well into Bonney Sandstone. Canyons were likely cut and filled syndepositionally with Ediacara Member.||Lowermost unit of Rawnsley Quartite.||Overlain by/infilled with Ediacara Member. Underlain unconformably by Bonney Sandstone.|Yellow weathering, pink coloured, felspathic, medium- to coarse grained sandstone with granule trains. Sets of low angle, trough crossbedding grade up into wavy and disrupted, thinly bedded sand.|26-JUN-19
68799|Chace Quartzite Member|68138|6|Mentioned|p156|Neoproterozoic|Neoproterozoic|Adelaide Rift Complex. Appears as Chace Quatzite Member.||Rawnsley Quartzite.||||
68799|Chace Quartzite Member|68271|5|Briefly described|p695|||Adelaide Rift Complex. Separated from underlying Billy Springs Formation via flooding surface.||||Underlain by Billy Springs Formation.|White sandstone.|
68799|Chace Quartzite Member|71250|6|Mentioned|p70|Ediacaran|Ediacaran|Central Flinders Ranges.||Rawnsley Quartzite.||Overlies Bonney Sandstone. Is overlain by Ediacara Member.||
40378|Challenger Gneiss|24296|5|Briefly described|p1258|Paleoproterozoic|Archean|Age: 2446 Ma (U-Pb). Geological Province: Gawler Craton.||||||01-MAR-10
40378|Challenger Gneiss|50130|5|Briefly described|p1, 10, 12|Paleoproterozoic|Archean|Protolith age: ca 2900 Ma (Nd model ages). Peak metamorphism: ca 2447 Ma. Geological Province: Christie Domain, Gawler Craton. Considered to be correlative with Christie Gneiss.||||||17-AUG-18
40378|Challenger Gneiss|66520|6|Mentioned|p10.|||Informal name of rock unit at Challenger Mine that includes volcaniclastic rocks.|c.2560 Ma zircon age.|||||
40378|Challenger Gneiss|73230|6|Mentioned|p8|||[Written as 'Challenger Gneiss']. Included in Christie Gneiss through convention.|||||Gneiss with volcaniclastic protolith.|
27309|Chandabooka Dacite|29838|2|Defined|p11|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27309|Chandabooka Dacite|30809|6|Mentioned|Fig.1|||||||||
27309|Chandabooka Dacite|35078|6|Mentioned|Fig.1|||||||||
27309|Chandabooka Dacite|35107|6|Mentioned|p199|||||||||
27309|Chandabooka Dacite|37461|6|Mentioned|p325|||||||||
27309|Chandabooka Dacite|39802|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
27309|Chandabooka Dacite|40241|6|Mentioned|p115|||||||||
27309|Chandabooka Dacite|40644|6|Mentioned|p136|Mesoproterozoic|Mesoproterozoic|Part of the widespread sheets of dacite and rhyodacite overlying the Chitanilga and Glyde Volcanic Complexes.||||||13-AUG-08
27309|Chandabooka Dacite|42368|5|Briefly described|p51|||||||||
27309|Chandabooka Dacite|42469|6|Mentioned|p16|||Gairdner, SH53-15||||||
27309|Chandabooka Dacite|42546|5|Briefly described|Map legend|Mesoproterozoic||||||||
27309|Chandabooka Dacite|42721|5|Briefly described|map legend|Carpentarian||||||||
27309|Chandabooka Dacite|42736|5|Briefly described|map legend|Mesoproterozoic||||||||
27309|Chandabooka Dacite|43052|5|Briefly described|p117|||Of Gawler Range Volcanics.||||||02-JUN-09
27309|Chandabooka Dacite|43094|4|Described|p20|||see also Table 2.||||||
27309|Chandabooka Dacite|67909|5|Briefly described|p126-128, 131|Mesoproterozoic|Mesoproterozoic|Kokatha area. Volcanic textures and emplacement mechanism tabulated. Volume >20 km3.||||Correlated with Yardea Dacite.||
27309|Chandabooka Dacite|70659|5|Briefly described|p6 fig 2, p8|Mesoproterozoic|Mesoproterozoic|Kokatha area.||Upper Gawler Range Volcanics.|||Dacite.|
27309|Chandabooka Dacite|70816|5|Briefly described|p5|||Kokatha area.||Unit of upper Gawler Range Volcanics.||Equivalent to Carnding Rhyodacite and Yardea Dacite.||
27309|Chandabooka Dacite|72090|6|Mentioned|p12|||Gawler Craton.||Gawler Range Volcanics, Upper||||
26473|Charleston Granite|22430|6|Mentioned|p2||Proterozoic|||||||
26473|Charleston Granite|22544|5|Briefly described|p136|Mesoproterozoic|Mesoproterozoic|||||||
26473|Charleston Granite|23719|4|Described|p23|Calymmian|Calymmian|Age: 1585+/-2 Ma(U-Pb zircon), see also page 15 table 2. Of Hiltaba Suite. Geological Province:  Gawler Craton.||||||
26473|Charleston Granite|23818|5|Briefly described|p30|||Geological Province: Gawler Block. Intrudes the Moonabie Formation and Moonabie Porphyry. Age: 1590 Ma.||||||23-JUL-13
26473|Charleston Granite|24197|5|Briefly described|p30, p74 Tb. 8.1|Mesoproterozoic|Mesoproterozoic|Of the Hiltaba Suite (Roxby Downs type). Age: 1592Ma. Geological Province: Gawler Craton.||||||07-FEB-11
26473|Charleston Granite|24217|5|Briefly described|p841|||Parent: Hiltaba Suite.   Geological Province: Gawler Craton||||||
26473|Charleston Granite|24381|5|Briefly described|p58|||Of Hiltaba Suite.||||||
26473|Charleston Granite|30237|6|Mentioned|Fig.1|||||||||
26473|Charleston Granite|30806|5|Briefly described|Table 1|||||||||
26473|Charleston Granite|30845|6|Mentioned|Fig.1|||||||||
26473|Charleston Granite|31034|6|Mentioned|p132|||Also mention P133.||||||
26473|Charleston Granite|31320|5|Briefly described|p19|||Carpentarian||||||
26473|Charleston Granite|32435|6|Mentioned|Fig.1|||||||||
26473|Charleston Granite|32436|6|Mentioned|p120|||||||||
26473|Charleston Granite|32437|6|Mentioned|Fig.2|||||||||
26473|Charleston Granite|32438|6|Mentioned|Fig.2|||||||||
26473|Charleston Granite|33004|6|Mentioned|p127|||||||||
26473|Charleston Granite|33224|6|Mentioned|p53|||Age date||||||
26473|Charleston Granite|33468|6|Mentioned|p205|||1590my||||||
26473|Charleston Granite|33479|6|Mentioned|Fig.1|||||||||
26473|Charleston Granite|33557|6|Mentioned|p10|||||||||
26473|Charleston Granite|34537|5|Briefly described|p30|||Carpentarian||||||
26473|Charleston Granite|35298|5|Briefly described|Table 1|||||||||
26473|Charleston Granite|35633|6|Mentioned|p32|||||||||
26473|Charleston Granite|36073|6|Mentioned|Fig.3|||||||||
26473|Charleston Granite|36627|4|Described|p85|||||||||
26473|Charleston Granite|37461|6|Mentioned|p325|||||||||
26473|Charleston Granite|38068|5|Briefly described|p66|||||||||
26473|Charleston Granite|39349|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
26473|Charleston Granite|39802|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
26473|Charleston Granite|40448|5|Briefly described|Table 4|||||||||
26473|Charleston Granite|40644|5|Briefly described|p124 Fig. 3, p136|Mesoproterozoic|Paleoproterozoic|Of the Hiltaba Suite.  Mostly Middle Proterozoic, but parts may be as old as Early Proterozoic.||||||07-NOV-08
26473|Charleston Granite|41667|4|Described|p72|||||||||
26473|Charleston Granite|41972|4|Described|p380|||||||||
26473|Charleston Granite|42235|6|Mentioned|p134|||||||||
26473|Charleston Granite|42468|5|Briefly described|p13|||||||||
26473|Charleston Granite|42469|6|Mentioned|p13|||Port Augusta, SI53-4||||||
26473|Charleston Granite|42716|6|Mentioned|Map legend|Mesoproterozoic||||||||
26473|Charleston Granite|42738|6|Mentioned|map legend|Mesoproterozoic||||||||
26473|Charleston Granite|42934|4|Described|p520|||Part of Hiltaba supersuite. Intrudes McGregor  Volcanics, Moonabie Formation and Corunna Conglomerate. I-type granite.||||||12-JAN-10
26473|Charleston Granite|43049|6|Mentioned|p15|||||||||
26473|Charleston Granite|43052|5|Briefly described|Table 5.6|||of Hiltaba Suite||||||
26473|Charleston Granite|43053|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of Hiltaba Suite. Anorogenic granitoids. Geological Province: Gawler Craton.||||||26-MAY-05
26473|Charleston Granite|43258|5|Briefly described|Map Legend||Mesoproterozoic|||||||
26473|Charleston Granite|43298|5|Briefly described|Map Legend||Mesoproterozoic|||||||
26473|Charleston Granite|45003|14|Not recorded|p19,47|||See also Lexicon||||||
26473|Charleston Granite|48894|6|Mentioned|p71|||1590+-30my||||||
26473|Charleston Granite|50605|5|Briefly described|p(ii), 1.3, 8.1, Table 1.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Gawler Craton & Curnamona Province. Of the Roxby Downs suite. Age: 1585-1576 +/- 5Ma (Shrimp, U-Pb).||||||
26473|Charleston Granite|60953|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of the Hiltaba Suite. Geological Province: Gawler Craton.||||||
26473|Charleston Granite|61108|5|Briefly described|map legend|Mesoproterozoic|Mesoproterozoic|Of Hiltaba Suite. Geological Province: Gawler Craton. Age: 1598-1575 Ma.||||||23-JUN-05
26473|Charleston Granite|61556|5|Briefly described|p9-10 Figure|Carpentarian|Carpentarian|In Middleback Range, Eyre Peninsula.||||||21-NOV-07
26473|Charleston Granite|62893|6|Mentioned|Map Legend|Middle Proterozoic|Middle Proterozoic|||||||
26473|Charleston Granite|63020|5|Briefly described|p987 Fig. 8|Mesoproterozoic|Mesoproterozoic|Age: 1585+/-5Ma. Geological Province: Gawler Craton (Spencer Domain).||||||10-AUG-07
26473|Charleston Granite|65376|6|Mentioned|p147.|||Range of inherited zircons implies that parts of the Hiltaba Suite, unlike Gawler Range Volcanics, are derived from melting of older Gawler Craton continental crust.||Unit in Hiltaba Suite.||||
26473|Charleston Granite|65390|6|Mentioned|p23 Fig.3, p26 Tb. 1|Calymmian|Calymmian|Spencer Domain, Gawler Craton. Of Hiltaba Suite. Homogeneous, coarse-grained, megacrystic granite. Intrudes McGregor Volcanics and Corunna Conglomerate. Has a U-Pb zircon age of 1585 +/- 5 Ma (Creaser and Fanning, in press); other age determinations listed.||||||
26473|Charleston Granite|65915|5|Briefly described|p5, p4 Fig.3, p16, p16 Fig.9, p18-19|Calymmian|Calymmian|Unit in Hiltaba Suite. ~1590 Ma.||||||
26473|Charleston Granite|66302|5|Briefly described|p47|Calymmian|Calymmian||1585 +/- 5 Ma (Creaser and Fanning, 1993)|||Intrudes the McGregor Volcanics and the Corunna Conglomerate.|Megacrystic granite.|
26473|Charleston Granite|67027|5|Briefly described|p351 Table 1.|Mesoproterozoic|Mesoproterozoic||1585 +/- 2 Ma (U-Pb : Parker and Fanning 1998).|||Intrudes Corunna Conglomerate.|Massive porphyritic granite.|
26473|Charleston Granite|67028|6|Mentioned|p362, p364, Tb.1|Calymmian|Calymmian|Information on magnetic characteristics presented. Roxby Downs-type.||Hiltaba Suite Granitoids||||10-AUG-15
26473|Charleston Granite|67900|5|Briefly described|p22|Mesoproterozoic|Mesoproterozoic|North-eastern Eyre Peninsula, Gawler Craton.||Hiltaba Suite.|||A more-evolved granite.|
26473|Charleston Granite|68208|6|Mentioned|p31 Fig.2, p32 Fig.3, p39|Mesoproterozoic|Mesoproterozoic|Hiltaba-aged, contains an inherited zircon with age in excess of c.3150 Ma and Nd model age of 2840 Ma, suggesting it was partially derived from or incorporated Cooyerdoo Granite at depth.|Crystallisation age ~1585 Ma.|||||
26473|Charleston Granite|71235|6|Mentioned|p9|Mesoproterozoic|Mesoproterozoic|||Hiltaba Suite||||
26473|Charleston Granite|71413|6|Mentioned|p31 Fig 1, p32 Fig 2|||Geological province: Gawler Craton. ||||||
26473|Charleston Granite|71536|6|Mentioned|p22, p24-p25|||||Hiltaba Suite||||
26473|Charleston Granite|71859|6|Mentioned|p18|Mesoproterozoic|Mesoproterozoic|||||||
26473|Charleston Granite|72058|4|Described|p170-p173,p174. p176. p178-p179|Mesoproterozoic|Mesoproterozoic|Gawler Craton. Occurs immediately south of the Middleback Ranges and forms bedrock over a 300km^2 area in the eastern Eyre Peninsula. Whole rock geochemistry is provided. Sample MB158 illustrated. See also p181, p184, p186, p190, p192.|~1600 Ma|||Equivalent to the Hiltaba Suite.|S-type granite composed of commonly perthitic K-feldspar, plagioclase, biotite and amphibole.|16-MAR-21
26473|Charleston Granite|72459|5|Briefly described|p8, p13, p51|Mesoproterozoic|Mesoproterozoic|Eyre Peninsula. Dates the minimum age for the last movement of the shear zone seperating the Moonta and Lincoln subdomains of the Gawler Craton. Appears as Charleston granite on p13. Appears as Charleston granite on p51.|1584 +/- 5 Ma, 1581 +/- 4 Ma|||||
26473|Charleston Granite|72484|6|Mentioned|p2-3|||Eyre Peninsula region, Gawler Craton. Post-Kimban Orogeny; Hiltaba-affiliated.|~1.6 Ga.|||||
26473|Charleston Granite|72949|6|Mentioned|p36|Calymmian|Calymmian|Olympic Domain, south. Yorke Peninsula / Eastern Eyre Peninsula.  A-type (alkali) granites.|1585 +/- 5 Ma|||||24-DEC-21
26473|Charleston Granite|73103|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic||||||Granite, homogeneous, coarse-grained, megacrystic granite.|
25843|Chinaman Gully Formation|22525|6|Mentioned|p35,37||Eocene|||||||
25843|Chinaman Gully Formation|22528|6|Mentioned|p43 Fig2||Late Eocene|||||||
25843|Chinaman Gully Formation|22541|4|Described|p 29, Fig 1, 3, 7|||||||||
25843|Chinaman Gully Formation|22587|6|Mentioned|p79 Fig.7|Late Eocene|Late Eocene|||||||
25843|Chinaman Gully Formation|23489|5|Briefly described|p43 Table 1|Oligocene|Eocene|||||||
25843|Chinaman Gully Formation|30250|6|Mentioned|p2|||See also Fig.2||||||
25843|Chinaman Gully Formation|35542|6|Mentioned|p2|||Correct spelling of Chinamans Gully.||||||
25843|Chinaman Gully Formation|35689|2|Defined|p19|late Eocene|late Eocene|Correct spelling of Chinamans Gully.||||||
25843|Chinaman Gully Formation|36127|5|Briefly described|p11|||See also p7.||||||22-AUG-18
25843|Chinaman Gully Formation|36244|6|Mentioned|p2|||Redefined by Cooper 1979.||||||
25843|Chinaman Gully Formation|36500|6|Mentioned|Fig.4|||||||||
25843|Chinaman Gully Formation|37324|6|Mentioned|p11|||||||||
25843|Chinaman Gully Formation|38107|4|Described|p30|||||||||
25843|Chinaman Gully Formation|38621|6|Mentioned|Table 1|||Refers Cooper 1979.||||||
25843|Chinaman Gully Formation|39351|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
25843|Chinaman Gully Formation|40238|6|Mentioned|p324|||||||||
25843|Chinaman Gully Formation|40429|6|Mentioned|p27|||||||||
25843|Chinaman Gully Formation|40453|6|Mentioned|p61|||||||||
25843|Chinaman Gully Formation|40778|6|Mentioned|p547|||||||||
25843|Chinaman Gully Formation|40877|5|Briefly described|p47|||||||||
25843|Chinaman Gully Formation|40969|6|Mentioned|Fig.1|||||||||
25843|Chinaman Gully Formation|40970|6|Mentioned|p16|||||||||
25843|Chinaman Gully Formation|41025|6|Mentioned|Fig.2|||||||||
25843|Chinaman Gully Formation|41495|5|Briefly described|Table 5|||||||||
25843|Chinaman Gully Formation|41513|6|Mentioned|p42|||||||||
25843|Chinaman Gully Formation|41517|6|Mentioned|p137|||||||||
25843|Chinaman Gully Formation|41520|4|Described|Fig.5|||||||||
25843|Chinaman Gully Formation|41626|6|Mentioned|p54|||||||||
25843|Chinaman Gully Formation|42443|6|Mentioned|p7|||St Vincent Basin||||||
25843|Chinaman Gully Formation|42498|5|Briefly described|Map Legend|Eocene|Eocene|||||||
25843|Chinaman Gully Formation|42506|5|Briefly described|Map legend|Eocene||Age Tertiary||||||
25843|Chinaman Gully Formation|42574|6|Mentioned|Fig.2 P242|||||||||
25843|Chinaman Gully Formation|42733|5|Briefly described|map legend|Tertiary||||||||
25843|Chinaman Gully Formation|44133|4|Described|p168, 165 Fig. 10.11|Early Oligocene|Late Eocene|Geological Province: Saint Vincent Basin. Thickness: 2m. Overlain disconformably by the Port Willunga Formation. Includes: Tandanya Sand Member.||||||
25843|Chinaman Gully Formation|60538|5|Briefly described|p479 Fig. 18|Oligocene|Eocene|Geological Province: Saint Vincent Basin.||||||
25843|Chinaman Gully Formation|61155|5|Briefly described|p3, p17|Late Eocene|Late Eocene|Lagoonal deposits. Overlies Blanche Point Formation; underlies Aldinga Member and Pirramimma Sand Member (Port Willunga Formation).  Age: 38-37Ma. Geological Province: St Vincent Basin.||||||
25843|Chinaman Gully Formation|61560|5|Briefly described|p499|Early Oligocene|Late Eocene|Contains spherules which have been replaced by zeolites and palagonite in the top levels.  Geological Province: St Vincent Basin (SA). ||||||
25843|Chinaman Gully Formation|64397|5|Briefly described|p232 Fig. 1A, p233|Oilgocene|Oilgocene|Varicoloured clay, silt, sand. Geological province: St Vincent Basin. See also p245 Fig. 11.||||||28-MAR-13
25843|Chinaman Gully Formation|65891|5|Briefly described|p221 Fig.5, p222 Fig.7,  p228-229.|Paleogene|Paleogene|St Vincent Basin. Coarse to fine siliciclastics occupying a c.50m downcut within silica-rich and dysaerobic facies of Blanche Point Formation. Underlies Aldinga Member. Rupelian age.||||||
25843|Chinaman Gully Formation|66131|6|Mentioned|p242 Fig.2|Eocene|Eocene|Late Eocene in age (from p.242 Fig.2 - stratigraphic correlation chart).||||Overlies Blanche Point Formation. Is overlain by Aldinga Member.||
25843|Chinaman Gully Formation|66187|5|Briefly described|p424|Late Eocene|Late Eocene|St Vincent Basin. Sediments of this unit contain a possible distal impact-related tsunami deposit.||||||
25843|Chinaman Gully Formation|66194|6|Mentioned|p584|Late Eocene|Late Eocene|St Vincent Basin. Marine.||||||09-MAR-12
25843|Chinaman Gully Formation|67462|5|Briefly described|Map legend.|Eocene|Eocene|Eastern Saint Vincent Basin.||||||
25843|Chinaman Gully Formation|68715|6|Mentioned|p31 Fig.5|Bartonian|Bartonian|St Vincent Basin.||||||
25843|Chinaman Gully Formation|70660|4|Described|p18, p3, p8-p9, p11-p12|Early Rupelian|Early Rupelian|Fossil assemblage includes leaves and foraminifera. See also  p17 fig 9a,  p25-p27, p32, p43. Grouped with overlying Aldinga Mmeber of Prot Willunga Fm  [evidence for asserted age not clear]|||Includes the Tandanya Sand Member.|Overlies the Blanche Point Formation, Tuit Member. Unconformably overlies the Gull Rock Member or Tuketja Member. Overlain by the Aldinga Member.|Sands, silts and clays that are brightly coloured in outcrop and darker and carbonaceous at depth.|22-AUG-18
25843|Chinaman Gully Formation|70722|5|Briefly described|p218|Late Eocene|Late Eocene|Of St. Vincent Basin. Equivalent to Kingscote Limestone Unit K1 of this study.||||Overlain by Port Willunga Formation. Underlain by Blanch Point Formation.||
25843|Chinaman Gully Formation|73188|5|Briefly described|p320, p337, p345, p351|Oligocene|Oligocene|St Vincent Basin.||||Disconformably underlain by Blanche Point Formation. Overlain by Port Willunga Formation.|Thin fluvial sands.|
34576|Chinmina Monzonite|22834|2|Defined|P39, P42||Statherian|New formation name, age of unit is 1702+/-10 Ma, intrudes Hutchison Group||||||
34576|Chinmina Monzonite|61070|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Moody Suite. Massive to weakly foliated, medium to coarse grained, dark grey-black monzonite with phenocrysts of plgioclase, microline and hornblende. Age: 1720 +/- 10Ma (U-Pb Zircon). Geological Province: Gawler Craton.||||||12-JAN-10
34576|Chinmina Monzonite|65376|5|Briefly described|p83, pp88-89.||||1701 +/- 12 Ma.|Unit in Moody Suite.|||Even-grained syenite to monzonite, massive to weakly foliated, medium- to coarse-grained, dark grey-black.|
34576|Chinmina Monzonite|66302|6|Mentioned|p27|Statherian|Statherian||1701 +/- 12 Ma (Fanning et al, 2007)|Moody Suite||||
34576|Chinmina Monzonite|71862|5|Briefly described|p7, p15, p17, p19-20, p24, p37, p39-p41|Statherian|Statherian|Exposed at Chinmina Hill and a road metal quarry near Kapinka Falls, 25km west-northwest from Tumby Bay. Originally the Chinmina Syenite of Schwarz (1999). The type locality is found at the quarry near Kapinka Falls and there it is cross cut by an unnamed pegmatite and fine-grained granitic dykes. Mistakenly referred to as the Chinmina Monzogranite on p20.|c. 1700 Ma|Moody Suite||Intrudes (interpreted) the Hutchison Group. Faulted against the Uranno Microgranite.|Homogenous medium- to coarse-grained hornblende monzonite with K-feldspar in a groundmass of feldspar, hornblende, biotite and quartz.|18-APR-23
24842|Christie Gneiss|22509|6|Mentioned|p20||Archean|||||||07-NOV-08
24842|Christie Gneiss|22613|3|Fully described|p10|||||||||
24842|Christie Gneiss|22614|5|Briefly described|map|||||||||
24842|Christie Gneiss|22629|6|Mentioned|p148|Archean|Archean|||||||07-NOV-08
24842|Christie Gneiss|22850|5|Briefly described|16|Archean|Archean|Geol province Gawler Craton.||||||02-JUN-09
24842|Christie Gneiss|22946|5|Briefly described|p9-10|Archean|Archean|||||||07-NOV-08
24842|Christie Gneiss|24296|5|Briefly described|p1249, p1250|Archean|Archean|Of the Mulgathing Complex. Age: ca. 2440 Ma. Geological Province: Gawler Craton.||||||07-NOV-08
24842|Christie Gneiss|24472|5|Briefly described|p5 Tb.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Harris Greenstone Domain, Gawler Craton. Age: 2440 Ma (metamorphic zircon age). Part of the Mulgathing Complex.||||||03-AUG-09
24842|Christie Gneiss|39802|6|Mentioned|Map legend|Archean|Archean|||||||07-NOV-08
24842|Christie Gneiss|40644|6|Mentioned|p120 Fig. 2, p126|Paleoproterozoic|Paleoproterozoic|Included in the Mulgathing Complex.  Age: 2417+/-59Ma. Geological province: Gawler Craton.||||||07-NOV-08
24842|Christie Gneiss|42465|5|Briefly described|Map Legend|||||||||
24842|Christie Gneiss|42468|5|Briefly described|p13|||Actually spelt Christie Gneisses.||||||
24842|Christie Gneiss|42469|4|Described|p10|||||||||
24842|Christie Gneiss|43052|4|Described|p38,Table 3.2|||Of Mulgathing Complex.||||||02-JUN-09
24842|Christie Gneiss|44695|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
24842|Christie Gneiss|44935|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
24842|Christie Gneiss|50130|5|Briefly described|p2|Archean|Archean|Basal unit of the Mulgathing Complex. Considered to correlate with the Challenger Gneiss.||||||07-NOV-08
24842|Christie Gneiss|50605|5|Briefly described|p8.7|||Of the Mulgathering Complex. Geological Province: Gawler Craton and Curnamona Province.||||||02-JUN-09
24842|Christie Gneiss|61659|4|Described|p28, p29, p31 Fig.2, pp37-39.    |||Gawler Craton. All lithologies were deformed by the Sleaford Orogeny between c.2.5 and 2.42 Ga. Generally low magnitude, bland magnetic signature. S.G. = 2.76 +/- 0.02.||Unit in Mulgathing Complex.|||Layered, weakly foliated, migmatitic paragneiss interlayered with felsic orthogneiss; semi-pelitic garnet-biotite gneiss; calc-silicate rock; mafic orthogneiss and metamorphosed banded iron formation.|
24842|Christie Gneiss|61836|5|Briefly described|p208, p210|Archean|Archean|Compositionally layered granulite facies metasediment; BIF predominates as most prominent and persistent outcrops. Geological Province: Gawler Craton.||||||07-NOV-08
24842|Christie Gneiss|62978|5|Briefly described|p164, p165|Archean|Archean|Metamorphosed sediments to granulite-facies. Ages: ~2440Ma and 2447Ma (metamorphic). Intruded by plutons of the Ifould Complex. Geological Province: Gawler Craton.||||||07-FEB-11
24842|Christie Gneiss|63866|4|Described|p3, p14-p15, p17|Archean|Archaean|Christie Domain, Gawler Craton. Metamorphosed in the earliest Proterozoic at 2480-2420. BIF, chert, carbonate, calc-silicate and aluminous metasediments in the Wilgena Domain are interpreted as low-grade equivalents; however, little geochronological data exists to support this correlation.||Mulgathing Complex||||
24842|Christie Gneiss|64130|6|Mentioned|p1379 |||Hosts the Challenger gold mine: premetamorphic, possible meso- or epithermal origin.||||||
24842|Christie Gneiss|64739|5|Briefly described|p266.|||All lithologies deformed by Sleaford Orogeny between c.2500 Ma and 2420 Ma.||Unit in Mulgathing Complex.|||Migmatitic paragneiss interlayered with felsic orthogneiss; garnet-biotite gneiss; calc-silicate rock; mafic orthogneiss; metamorphosed banded iron formation.|
24842|Christie Gneiss|65376|5|Briefly described|p190, pp198-200. |||||Unit in Mulgathing Complex.|||Compositionally layered metasedimentary rocks: garnet-rich paragneiss, green and black banded iron-formation, basic gneiss; includes interlayered quartzite, layered calc-silicate, marble.|
24842|Christie Gneiss|65385|5|Briefly described|pS131 Tab.2, pS132|Neoarchean|Neoarchean|Of Mulgathing Complex. Volcaniclastic protolith dated at ~2520 Ma (McFarlane et al., 2007).||||||08-MAR-12
24842|Christie Gneiss|65390|5|Briefly described|p14, p22 Fig. 3|Archean|Archean|Of Mulgathing Complex, Gawler Craton. Aluminous metasediments. Hosts Challenger gold deposit. Age >2440 Ma. Syn-tectonic with Glenloth Granite.||||||
24842|Christie Gneiss|65772|6|Mentioned|p231|Late Archean|Late Archean|Intruded by, and forms extensive enclaves within, Tunkillia Suite.||||||
24842|Christie Gneiss|66302|4|Described|p10, p11, p21, p23, p61, p61 Fig.14|Neoarchean|Neoarchean|Underwent granulite facies metamorphism during the Sleafordian Orogeny (2447 +/- 9 Ma). Protolith interpreted to have been deposited in a shallow to moderate depth marine environment in an extensional back arc setting. Also partially derived from pre-existing continental basement.  Ages from Jagodzinski et al. (2009).|2514 +/- 4 Ma to 2484 +/- 7 Ma |Mulgathing Complex||Is equivalent to the Sleaford Complex.|Metasedimentary rocks, including banded iron formation, chert, carbonate, calc-silicate, quartzite and aluminous sedimentary rocks.|
24842|Christie Gneiss|67058|5|Briefly described|p476, p492.|Neoarchean|Neoarchean|Central Gawler Craton.|c.2530 Ma.|Unit in Mulgathing Complex.||||
24842|Christie Gneiss|67483|5|Briefly described|p190|Archean|Archean|Compositionally-layered. Has undergone multiple deformations and metamorphism to granulite facies. Typically highly weathered to tens of metres depth.||||||
24842|Christie Gneiss|67980|5|Briefly described|p561 Tb.3, p564|Paleoproterozoic|Paleoproterozoic|Christie Domain, Gawler Craton. Several U-Pb zircon ages given for maximum deposition, cooling, metamorphism. Youngest detrital zircon age: 2480+/-4 Ma. Metamorphic ages: 2428- 2469 Ma.||||||08-FEB-17
24842|Christie Gneiss|68128|4|Described|p2-p3, p7, p13-14, p19-20, p22, |Palaeoproterozoic|Archaean|Gawler Craton. Deposited in a shallow to moderate water depth environment interpreted to have been a restricted, actively subsiding basin. Additional SHRIMP ages include 2512 +/- 5 Ma and 2488 +/- 7 Ma. Type area is at Mt Christie. Outcrops are sparse. Sample locations, zircon morphology, SHRIMP analyses and results are discussed. See also p27-28, p38, p42-43, p58, p71, p83-84, p109, p113.|2480 +/- 4 Ma (SHRIMP U-Pb)|Mulgathing Complex|||Migmatitic gneiss, local paragneiss, carbonates, calcsilicates, quartzite and banded iron formation.|01-FEB-23
24842|Christie Gneiss|68131|6|Mentioned|p77|Paleoproterozoic|Archean|||||||
24842|Christie Gneiss|68208|6|Mentioned|p31 Fig.2|Paleoproterozoic|Neoarchean|||Of Mulgathing Complex||||
24842|Christie Gneiss|69004|5|Briefly described|p39|Archean|Archean|Northern Gawler Craton. Hosts lode gold mineralisation.|||||Cordierite-bearing metasedimentary rocks.|
24842|Christie Gneiss|69048|5|Briefly described|p18||Paleoproterozoic||2480 +/- 4 Ma (maximum deposition age).|Mulgathing Complex.|||Metasedimentary rocks.|08-FEB-17
24842|Christie Gneiss|69213|5|Briefly described|p29, 24|Paleoproterozoic|Neoarchean|Gawler Craton. Type locality at Mount Christie discussed, also occurrence at Challenger [gold] mine. Encompasses all metasedimentary lithologies of Mulgathing Complex. Gold is present in some areas, occuring in leucosomes and peak metamorphic garnets. |2555-2485 Ma|Mulgathing Complex|||Gneiss and meta-banded iron formations interlayered with stromatic migmatite that contains abundant coarse-grained, poikiloblastic garnet, cordierite, K-feldspar, biotite and quartz.|
24842|Christie Gneiss|69648|6|Mentioned|p13|||Christie Subdomain, western Gawler Craton. Occurrences of Mulgathing Complex on sheets adjacent to OOLDEA have been subdivided into several Formations and Members, including paragneisses of Christie Gneiss.||Mulgathing Complex||||
24842|Christie Gneiss|69649|5|Briefly described|p35|Archean|Archean|Harris Greenstone Domain.|||||Aluminous metasediments.|
24842|Christie Gneiss|70027|5|Briefly described|p58|Paleoproterozoic|Neoarchean|Geological province: Gawler Craton. Represents BIF deposition ca. 2560-2470 Ma. |ca. 2560-2470 Ma.|||Interlayered with Mulgathing Complex.|Metamorphosed BIF and calc-silicate units.|
24842|Christie Gneiss|71536|6|Mentioned|p141|||||||||
24842|Christie Gneiss|71859|5|Briefly described|p2, p28|||Central-western Gawler Craton.||Mulgathing Complex.|||Banded iron-formation, carbonates and extensive clastic sequences; metasedimentary rocks.|
24842|Christie Gneiss|73155|6|Mentioned|p283|Archean|Archean|||Mulgathing Complex||||
24842|Christie Gneiss|73230|4|Described|p4, p6-8, p10-16|Siderian|Siderian|Gawler Craton. Domain: Christie and Wilgena. Includes 'Challenger Gneiss'. Most extensive formation of the Mulgathing Complex; occurs over a more than 25,000 km2 arcuate belt. Hosts Challenger and Golf Bore gold deposits and iron mineralisation. Low magnetic response. Metamorphosed to amphibolite-granulite facies at c. 2470-2415 Ma [also written as c. 2470-2440 Ma]. [Lithological] distinction from Kenella Gneiss may be somewhat unclear.|c. 2485-2480 Ma (maximum deposition)|Mulgathing Complex|George Hill Iron Member|Intruded by Aurora Tank Suite, Mobella Tonalite, Burden Metagabbro, Aristarchus Metaperidotite, and Skuse Hill Metapyroxenite.|Predominantly metasedimentary gneiss with migmatitic layers. Paragneiss, magnetite gneiss, marble, calcsilicate and quartzite with minor volcaniclastic and mafic lithologies.|
24842|Christie Gneiss|73235|6|Mentioned|p56|||Hosts Challenger, Gold Bore mineralisation in the Christie mineral field and Hilga South, Birthday gold mineralisation in the Hilga mineral field of the Sleafordian gold mineral system.|||||[May include sediments, felsic intrusives, mafic and ultramafic rocks, and banded iron formations].|
26477|Christine Judith Conglomerate|22631|6|Mentioned|p177|||||||||
26477|Christine Judith Conglomerate|22772|4|Described|p64,Table13.1|Cryogenian|Cryogenian|||||||
26477|Christine Judith Conglomerate|22857|5|Briefly described|p64, Tb. 13.1 (insert p70-71)|Willouran|Willouran|Of the Pintapah Subgroup (Poolamacca Group). Rounded, well-sorted quartzite pebbles and cobbles in quartzite matrix. Age: >802+/-10Ma based on correlation with SA. Max. thickness: 150m. Geological Province: Adelaide Fold Belt. See also p400 App. 1 Tb.A1.3.||||||29-AUG-18
26477|Christine Judith Conglomerate|30261|4|Described|Table 1|||Willouran age||||||
26477|Christine Judith Conglomerate|33004|6|Mentioned|p134|||||||||
26477|Christine Judith Conglomerate|34812|3|Fully described|p55|||||||||
26477|Christine Judith Conglomerate|35199|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
26477|Christine Judith Conglomerate|35692|6|Mentioned|p23|||||||||
26477|Christine Judith Conglomerate|36411|6|Mentioned|p268|||Refs Cooper et al. 1978 for definition.||||||
26477|Christine Judith Conglomerate|36733|6|Mentioned|Table 5|||||||||
26477|Christine Judith Conglomerate|37854|6|Mentioned|Table 1|||||||||
26477|Christine Judith Conglomerate|37931|4|Described|p533|||||||||
26477|Christine Judith Conglomerate|38157|6|Mentioned|Table II|||||||||
26477|Christine Judith Conglomerate|39214|6|Mentioned|p5|||||||||
26477|Christine Judith Conglomerate|40294|6|Mentioned|Table 2|||||||||
26477|Christine Judith Conglomerate|40595|6|Mentioned|Table 3|||||||||
26477|Christine Judith Conglomerate|41403|4|Described|p48|||||||||
26477|Christine Judith Conglomerate|42222|6|Mentioned|p11|||||||||
26477|Christine Judith Conglomerate|42223|6|Mentioned|Fig.2 P36|||||||||
26477|Christine Judith Conglomerate|42531|5|Briefly described|Map legend|Adelaidean||||||||
26477|Christine Judith Conglomerate|42813|6|Mentioned|p14|||||||||
26477|Christine Judith Conglomerate|43265|5|Briefly described|Map Legend||Neoproterozoic|of Pintapah Subgroup.||||||
26477|Christine Judith Conglomerate|43268|5|Briefly described|Map Legend||Neoproterozoic|of Pintapah Subgroup.||||||
26477|Christine Judith Conglomerate|43269|5|Briefly described|Map Legend||Neoproterozoic|of Pintapah Subgroup.||||||
26477|Christine Judith Conglomerate|62724|5|Briefly described|p17 Fig. 4|Willouran|Willouran|Of the Poolamacca Group. Geological Province: Broken Hill Domain.||||||07-FEB-11
26477|Christine Judith Conglomerate|69023|6|Mentioned|p63|||||||||
26477|Christine Judith Conglomerate|70000|5|Briefly described|p34|Neoproterozoic|Neoproterozoic|||Unit in Pintapah Subgroup.|||Fluviatile to shallow marine conglomerate.|
26477|Christine Judith Conglomerate|70015|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Mineral deposits (if any) are shown.||Unit in Pintapah Subgroup.||Overlies Lady Don Quartzite. Is overlain by Boco Formation.|Monomictic conglomerate with rounded, well-sorted quartzite pebbles and cobbles in a quartzite matrix.|07-SEP-15
26477|Christine Judith Conglomerate|72461|6|Mentioned|p16 fig 9|||||Pintapah Subgroup||||
24843|Christmas Rocks Microgranite|42275|6|Mentioned|Table 2 p474|||Geochemical analysis given.||||||23-AUG-18
75847|Cleve Group|66882|4|Described|p103-104 Figs.3c,4; p114-117, p119-121|Statherian|Statherian|Mixing of source components; Late Archean to Late Paleoproterozoic felsic, differentiated upper continental crust. Deposited at least c.70 million years after Darke Peak Group.|1780-1730 Ma||Contains Yadnarie Schist, Mount Shannon Iron Formation and Mangalo Schist.|Disconformably overlies Darke Peak Group.|Succession of dominantly psammitic and pelitic units.|
75847|Cleve Group|67900|6|Mentioned|p20|Paleoproterozoic|Paleoproterozoic|Szpunar et al. (2011). Eastern Gawler Craton.|c.1780 Ma.|||||
75847|Cleve Group|70027|6|Mentioned|p56-57|Statherian|Statherian|Geological province: Gawler Craton. Deposited at ca. 1790 Ma.|ca. 1790 Ma|||||
75847|Cleve Group|71322|5|Briefly described|p3, p104, p108, p119, p135|Paleoproterozoic|Paleoproterozoic|Szpunar et al., 2011. Cleve Domain. Formerly of the Hutchison Group. Age range given as c.1790-1740 Ma. Deformed c.1693 Ma during the Kimban Orogeny. Underwent hydrothermal (skarn) alteration at 1581 +/- 9 Ma.|c.1739 Ma (maximum depositional age of sample).|||Overlies Sleaford Complex.|Includes quartz-feldspar-sillimanite gneiss, migmatised.|14-DEC-21
75847|Cleve Group|71341|6|Mentioned|p196|||Broadly geochemically similar to the Myola Volcanics, McGregor Volcanics, Price Metasediments, Moonabie Formation and the Wallaroo Group. ||||||
75847|Cleve Group|73026|5|Briefly described|p6-7, p14, p25, p29|Paleoproterozoic|Paleoproterozoic|Central/western Eyre Peninsula. Seperated out from the Hutchison Group by Szpunar et al(2011) on the basis of zircon studies.|c. 1790-1750 Ma|||||
75847|Cleve Group|73027|5|Briefly described|p6-p7, p9, p14|Statherian|Statherian|Central/western Eyre Peninsula. See also p40, p43. Rocks belonging to this group previously belonged to the Hutchison Group.|c. 1780-1730 Ma|Hutchison Supergroup|||Metapelite.|
75847|Cleve Group|73122|6|Mentioned|p19|Palaeoproterozoic|Palaeoproterozoic|||||||
75847|Cleve Group|73234|6|Mentioned|p19|Statherian|Statherian|Age approximates deposition.|c. 1780-1730 Ma|||||
75847|Cleve Group|73235|6|Mentioned|p53, p58|Statherian|Statherian|Gawler Craton. Cleve, Coulta, Gawler Range Volcanic regions. Hosts Weednanna and Bartel orogenic gold mineralisation in the Cleve mineral field of the Kimban gold mineral system.|1790 Ma||||[May include schist, quartzite, and carbonates].|
75847|Cleve Group|73516|5|Briefly described|p11|Paleoproterozoic|Paleoproterozoic||||||Metasediments. Amphibolite to granulite grade metamorphism.|
75847|Cleve Group|73525|5|Briefly described|p19 Fig.13, p20|Statherian|Statherian|Cleve Domain.|1796+/-6 Ma, 1784+/-18 Ma||||Siliciclastics,|
36792|Cleve kimberlite|23772|5|Briefly described|p764||Jurassic|Age: 180 Ma.||||||
23492|Coads Hill Member|36495|2|Defined|p118|Early Cambrian|Early Cambrian|||||||
23492|Coads Hill Member|37802|6|Mentioned|Fig.2|||||||||
23492|Coads Hill Member|38108|6|Mentioned|Table 1|||||||||
23492|Coads Hill Member|42269|5|Briefly described|p336|||||||||
23492|Coads Hill Member|44133|4|Described|p4 Fig. 7.2, 26|Early Cambrian|Early Cambrian|Geological Province: Arrowie Basin. Of the Billy Creek Formation. Correlated with upper Oraparinna Shale. Also found beneath Billy Creek Formation. Maximum Thickness: 200m.||||||
23492|Coads Hill Member|60889|5|Briefly described|p245 Fig.2, p252 Fig.10|Early Cambrian|Early Cambrian|Shown as Coads Hill Mbr. Arrowie Basin.||Billy Creek Formation||Overlies (unconformably?) Moorowie Formation.||21-SEP-17
23492|Coads Hill Member|60959|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of the Billy Creek Formation. Conglomerate with cobbles of the Bendieuta Formation in coarse grained sandy matrix; sandstone, siltstone, shale, limestone.||||||
23492|Coads Hill Member|62270|5|Briefly described|p496, p502, p509 Fig. 8|Early Cambrian|Early Cambrian|Of the Billy Creek Formation. Contains Emuellids (Trilobite family).||||||
23492|Coads Hill Member|63569|6|Mentioned|p117 Fig.1|Early Cambrian|Early Cambrian|Arrowie Basin.||?of Billy Creek Formation.||||
23492|Coads Hill Member|65686|5|Briefly described|p409 Fig 2|Early Cambrian|Early Cambrian|||Of Billy Creek Formation.||Underlies the Edeowie Limestone Member, overlies the Moorowie Formation.||07-MAY-12
23492|Coads Hill Member|65892|6|Mentioned|p7 Fig.3. |Early Cambrian|Early Cambrian|Arrowie Basin. ||Unit in Billy Creek Formation.||||
23492|Coads Hill Member|65925|5|Briefly described|p14 Fig.2.2, Appendix 2.|Early Cambrian|Early Cambrian||||||Pale brown, fine- to medium-grained sandstone; dark grey limestone; red and green shale; shaly siltstone. Conglomerate at the base. Some tuff beds.|
33836|Colbert Granite|22489|5|Briefly described|p13|Proterozoic|Proterozoic|Of Donnington Granitoid Suite.||||||
33836|Colbert Granite|61070|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Donington Suite. Granite and granite gneiss intruding megacrystic granite of the Donington Suite.  Age: 1852.5 +/- 4.4Ma (U-Pb Zircon). Geological Province: Gawler Craton.||||||12-JAN-10
33836|Colbert Granite|64313|6|Mentioned|p450|Paleoproterozoic|Paleoproterozoic|Formerly known as the Colbert Suite (Mortimer et al 1988a; Hoek and Schaefer 1998; Schwarz, 2003). Included in the Donington Suite. Geological province: Gawler Craton.||||||09-FEB-10
33836|Colbert Granite|65375|6|Mentioned|p15.|||Considered equivalent to the syenogranite phase of the Gleesons Landing Granite.|1852 +/- 4.4 Ma.|||||
33836|Colbert Granite|65376|4|Described|p65, pp69-71.|||Previously named Colbert Suite; less deformed, cross-cutting dyke-like bodies in Donington Suite, but indistinguishable in their magmatic crystallisation age.|1853 +/- 5 Ma.|Unit in Donington Suite.||Intrudes Memory Cove Charnockite.|Ranges from equigranular, medium-grained, alkali feldspar-biotite(-hornblende) gneissic granite to variably foliated, medium-grained to porphyritic hornblende granite.|
33836|Colbert Granite|65390|6|Mentioned|p20|Orosirian|Orosirian|Dated at ~1850 Ma. Relatively undeformed, but includes foliated enclavesof megacrystic granite gneiss (Neill Event).||||||
33836|Colbert Granite|66302|6|Mentioned|p27|Orosirian|Orosirian||1853 +/- 5 Ma (SHRIMP, Fanning et al, 2007)|Donington Suite||||
33836|Colbert Granite|70721|6|Mentioned|p63|||Intruded and deformed during the Carnian Orogeny at c. 1850 Ma.||||||
33836|Colbert Granite|71859|5|Briefly described|p1|||Southern Gawler Craton.||||||
33836|Colbert Granite|71862|6|Mentioned|p2|||Originally a part of the now obsolete Lincoln Complex.||||||
33836|Colbert Granite|73525|5|Briefly described|p19 Fig.13|Orosirian|Orosirian|Spencer Domain.|1853+/-5 Ma crystallisation age|Donington Suite|||Felsic intrusive.|
41194|Coleraine Volcanic Group|50154|2|Defined|p25, p107, p130|Late Jurassic|Early Jurassic|Overlies the Hassall Creek Granodiorite, Bacchus Marsh Formation and the Glenelg River Metamorphic Complex. Disconformably overlain by the Otway Group, Parilla Sand and Lowan Sand. Intrudes the Bacchus Marsh Formation. Max. Thickness: 75m.||||||25-SEP-09
41194|Coleraine Volcanic Group|50155|5|Briefly described|Map Legend|Jurassic|Jurassic|Includes: Hypatia Formation and Den Hills Formation||||||
41194|Coleraine Volcanic Group|50156|5|Briefly described|Map Legend|Jurassic|Jurassic|Includes: Den Hills Formation, Hypatia Formation.||||||
41194|Coleraine Volcanic Group|50157|5|Briefly described|Map Legend|Jurassic|Jurassic|Includes: Den Hills Formation, Hypatia Formation.||||||
41194|Coleraine Volcanic Group|50158|5|Briefly described|Map Legend|Jurassic|Jurassic|Includes: Den Hills Formation, Hypatia Formation.||||||
41194|Coleraine Volcanic Group|50159|5|Briefly described|Map Legend|Jurassic|Jurassic|Includes: Den Hills Formation, Hypatia Formation.||||||
41194|Coleraine Volcanic Group|50160|5|Briefly described|Map Legend|Jurassic|Jurassic|Includes: Den Hills Formation, Hypatia Formation.||||||
41194|Coleraine Volcanic Group|50161|5|Briefly described|Map Legend|Jurassic|Jurassic|Includes: Den Hills Formation, Hypatia Formation.||||||22-JUN-04
41194|Coleraine Volcanic Group|50162|5|Briefly described|Map Legend|Jurassic|Jurassic|Includes Hypatia Formation and Den Hills Formation||||||
41194|Coleraine Volcanic Group|50163|5|Briefly described|Map Legend|Jurassic|Jurassic|Includes: Den Hills Formation, Hypatia Formation.||||||16-MAY-13
41194|Coleraine Volcanic Group|50164|5|Briefly described|Map Legend|Jurassic|Jurassic|Includes: Den Hills Formation, Hypatia Formation.||||||
41194|Coleraine Volcanic Group|60421|5|Briefly described|p408 Fig. 1, 409, 418 Fig. 5|Jurassic|Jurassic|Alkalic volcanics.||||||
41194|Coleraine Volcanic Group|64612|6|Mentioned|p28|Mesozoic|Mesozoic|||||||07-FEB-11
41194|Coleraine Volcanic Group|66002|5|Briefly described|p9 Tb.6|Mesozoic|Mesozoic|Includes Den Hills Formation and Hypatia Formation.  Defined by Morand et al. 2003. Previously called Coleraine trachyte by Hogg (1899)||||||
41194|Coleraine Volcanic Group|68116|5|Briefly described|Appendix, Maps 38-39.|Jurassic|Jurassic||||||Trachyte and basalt: lava flows, lava domes and laccoliths.|
27129|Colinlea Sandstone|13516|5|Briefly described|p145 fig 3, p147 fig 5|Late Permian|Late Permian|From western margin, Bowen Basin, Galilee Basin. Age: APP4 - APP5||||||
27129|Colinlea Sandstone|23982|6|Mentioned|p96 Appendix 13|||Geological Province: Great Artesian Basin.||||||
27129|Colinlea Sandstone|24071|5|Briefly described|p318|Late Permian|Early Permian|Geological Province: Galilee Basin.||||||
27129|Colinlea Sandstone|29411|5|Briefly described|p201|||||||||
27129|Colinlea Sandstone|29721|6|Mentioned|p65|||||||||
27129|Colinlea Sandstone|30102|6|Mentioned|p9|||||||||
27129|Colinlea Sandstone|30508|6|Mentioned|p91|||Reservoir potential. Stratigraphic drilling||||||
27129|Colinlea Sandstone|30691|4|Described|p6|||See also P14,20-22,Table 3,6. Permian age||||||
27129|Colinlea Sandstone|30914|6|Mentioned|Map legend|Permian|Permian|||||||
27129|Colinlea Sandstone|30915|6|Mentioned|Table|||Shown on table for stratigraphic drilling||||||
27129|Colinlea Sandstone|30916|6|Mentioned|p99|||||||||
27129|Colinlea Sandstone|31120|4|Described|p151|||||||||
27129|Colinlea Sandstone|31121|6|Mentioned|p388|||||||||
27129|Colinlea Sandstone|31122|6|Mentioned|p344|||Overlies Joe Joe Group||||||
27129|Colinlea Sandstone|31258|6|Mentioned|p98|||||||||
27129|Colinlea Sandstone|31260|6|Mentioned|p16|||Refers facies analysis||||||
27129|Colinlea Sandstone|32493|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
27129|Colinlea Sandstone|32577|5|Briefly described|p23|||||||||
27129|Colinlea Sandstone|32639|6|Mentioned|p76|||||||||
27129|Colinlea Sandstone|33078|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
27129|Colinlea Sandstone|33079|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
27129|Colinlea Sandstone|33086|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
27129|Colinlea Sandstone|33092|5|Briefly described|p7|||Strat. table||||||
27129|Colinlea Sandstone|33096|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
27129|Colinlea Sandstone|33366|6|Mentioned|Fig.3|||Perm.||||||
27129|Colinlea Sandstone|33368|6|Mentioned|p213|||Strat. succession GSQ Jericho 1.||||||
27129|Colinlea Sandstone|33369|6|Mentioned|p213|||Strat. succession in GSQ Jericho 1||||||
27129|Colinlea Sandstone|33372|5|Briefly described|p22|||Correlative described from wells.||||||
27129|Colinlea Sandstone|33639|6|Mentioned|Fig.1|||See also P10.||||||
27129|Colinlea Sandstone|33640|6|Mentioned|Table 4|||||||||
27129|Colinlea Sandstone|33646|6|Mentioned|p10|||Palynological stage.||||||
27129|Colinlea Sandstone|33648|6|Mentioned|p17|||Palynological divisions||||||
27129|Colinlea Sandstone|33674|6|Mentioned|Fig.1|||||||||
27129|Colinlea Sandstone|33675|4|Described|p411|||Lithology.||||||
27129|Colinlea Sandstone|34132|6|Mentioned|p5|||Upper Permian||||||
27129|Colinlea Sandstone|34138|6|Mentioned|Cor.Chart|||Artinskian - Kungurian||||||
27129|Colinlea Sandstone|34174|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
27129|Colinlea Sandstone|34390|4|Described|Table 2|||Permian. Gebbie Subgroup.||||||
27129|Colinlea Sandstone|34392|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
27129|Colinlea Sandstone|35457|4|Described|p629|||Also Fig.4 biostratigraphic relationships.||||||
27129|Colinlea Sandstone|35562|6|Mentioned|Table 5|||Biostratigraphy||||||
27129|Colinlea Sandstone|35845|6|Mentioned|p73|||See also Fig.25||||||
27129|Colinlea Sandstone|35937|6|Mentioned|p621|||||||||
27129|Colinlea Sandstone|36243|6|Mentioned|Table 3A|||||||||
27129|Colinlea Sandstone|36739|6|Mentioned|p21|||||||||
27129|Colinlea Sandstone|36921|4|Described|p184|||See also Table 1.||||||
27129|Colinlea Sandstone|37096|6|Mentioned|p248|||||||||
27129|Colinlea Sandstone|37451|6|Mentioned|Table 2|||||||||
27129|Colinlea Sandstone|37610|4|Described|p302|||||||||
27129|Colinlea Sandstone|39252|5|Briefly described|p20|||||||||
27129|Colinlea Sandstone|39261|6|Mentioned|Fig. 9|||||||||
27129|Colinlea Sandstone|39264|6|Mentioned|Fig. 13|||||||||
27129|Colinlea Sandstone|39445|5|Briefly described|Table 8|||||||||
27129|Colinlea Sandstone|39478|6|Mentioned|Table 1|||||||||
27129|Colinlea Sandstone|39754|6|Mentioned|p1690|||||||||
27129|Colinlea Sandstone|39942|6|Mentioned|p465|||||||||
27129|Colinlea Sandstone|39943|6|Mentioned|Table 5A|||||||||
27129|Colinlea Sandstone|40123|6|Mentioned|p465|||||||||
27129|Colinlea Sandstone|40623|5|Briefly described|p110|||||||||
27129|Colinlea Sandstone|41097|6|Mentioned|p165|||||||||
27129|Colinlea Sandstone|41116|4|Described|p433|||Briefly described Table 1||||||
27129|Colinlea Sandstone|41246|6|Mentioned|Map legend|Permian||||||||
27129|Colinlea Sandstone|41707|6|Mentioned|Fig.8|||||||||
27129|Colinlea Sandstone|41710|6|Mentioned|p222|||See also Fig.2||||||
27129|Colinlea Sandstone|42250|6|Mentioned|Fig.3 P30|||||||||
27129|Colinlea Sandstone|42256|6|Mentioned|Fig.1 P243|||||||||
27129|Colinlea Sandstone|42446|6|Mentioned|p1|||||||||
27129|Colinlea Sandstone|42447|6|Mentioned|Fig. 2|||||||||
27129|Colinlea Sandstone|42614|5|Briefly described|p14|||Galilee Basin||||||
27129|Colinlea Sandstone|42641|5|Briefly described|p108|||||||||
27129|Colinlea Sandstone|42856|6|Mentioned|p643|||||||||
27129|Colinlea Sandstone|42999|5|Briefly described|Table 1,p90|Late Permian|Late Permian|||||||21-DEC-11
27129|Colinlea Sandstone|43105|5|Briefly described|p13|||||||||
27129|Colinlea Sandstone|43114|6|Mentioned|Table 2|||||||||
27129|Colinlea Sandstone|43204|5|Briefly described|Map Legend|Late Permian|Late Permian|in the Denison Trough||||interfingers with Aldebaran Sandstone in part||23-DEC-11
27129|Colinlea Sandstone|43213|5|Briefly described|p10, p69, p154|Permian|Permian|Mollan et al. (1969). Crops out along the W flank of Denison Trough, across the Springsure Shelf, and along E flank of Galilee Basin. Correlated with upper Aldebaran Sandstone-Catherine Sandstone interval.|||||Fine- to medium-grained quartz sandstone and granule to cobble conglomerate, grading to pebbly sandstone.|
27129|Colinlea Sandstone|43812|6|Mentioned|Fig.3,p145|||||||||
27129|Colinlea Sandstone|43987|14|Not recorded|p267,270,278|||||||||
27129|Colinlea Sandstone|43994|14|Not recorded|Map Legend|||||||||
27129|Colinlea Sandstone|44172|14|Not recorded|Fig.1,T.1,p1332,1343|Kungurian|Artinskian|Equivalent to Catherine Sandstone, Freitag Formation and Ingelara Formation. Denison Trough||||||
27129|Colinlea Sandstone|44173|14|Not recorded|p11,112|||Basal part may be partly equivalent to Freitag Formation.||||||
27129|Colinlea Sandstone|44337|5|Briefly described|Map Legend|Late Permian|Early Permian|Lithology.||||||
27129|Colinlea Sandstone|44424|14|Not recorded|p293-301|||Represents Gebbie Subgroup on Springsure Shelf.||||||
27129|Colinlea Sandstone|44697|14|Not recorded|p91|||||||||
27129|Colinlea Sandstone|44700|14|Not recorded|p108|||Jericho No.1 well.||||||
27129|Colinlea Sandstone|45071|6|Mentioned|p32|||||||||
27129|Colinlea Sandstone|45073|5|Briefly described|p42|||Stratigraphy P58||||||
27129|Colinlea Sandstone|46849|6|Mentioned|Fig. 7|||||||||
27129|Colinlea Sandstone|48626|14|Not recorded|p22|||||||||
27129|Colinlea Sandstone|48900|2|Defined|p32|Early Permian|Early Permian|||||||
27129|Colinlea Sandstone|48920|3|Fully described|p23|||Permian age||||||
27129|Colinlea Sandstone|63713|5|Briefly described|p1507-1508, p1523, p1528|Wordian|Roadian|Eastern margin, Galilee Basin. Predominantly fluvial. On the E edge of the Springsure Shelf, this unit's name refers collectively to the upper Aldebaran Sandstone, Freitag and Ingelara Formations, and Catherine Sandstone. Well-log correlation.||||Is overlain by Peawaddy Formation.||
27129|Colinlea Sandstone|63832|6|Mentioned|p131 fig 2|Guadalupian|Guadalupian|Of Galilee Basin.||||||
27129|Colinlea Sandstone|64288|5|Briefly described|p532 Fig.1 |Wordian|Kungurian|||||Is overlain by Peawaddy Formation.||
27129|Colinlea Sandstone|64631|5|Briefly described|p44 Fig.2.|Wordian|Roadian|Galilee Basin. Biostratigraphic age control for base and top.||||Is overlain by Peawaddy Formation.||
27129|Colinlea Sandstone|64665|6|Mentioned|p53 Fig.2.|Late Permian|Middle Permian|Galilee Basin. Equivalent to Catherine Sandstone.||||||
27129|Colinlea Sandstone|65113|5|Briefly described|p349||Late Permian|Basal part of thin succession in Galilee Basin, west of Denision Trough. Equivalent to upper Aldebaran Sandstone. Whole succession continues up to Middle Triassic, but how much of this is Colinlea Sanstone is unclear.||||||
27129|Colinlea Sandstone|66188|6|Mentioned|431, Fig 3|Early Triassic|Late Permian|||||||
27129|Colinlea Sandstone|67323|5|Briefly described|p84|Permian|Permian|Eastern Galilee Basin.||||Correlated with Betts Creek beds.||
27129|Colinlea Sandstone|67402|4|Described|p43 tbl HPB1, p124 fig GLL1|Capitanian|Roadian|Galilee Basin. Highly prospective reservoir unit for the storage of carbon dioxide; has an estimated theoretical storage capacity of 1320 Megatonnes of carbon dioxide. At least 64m thick in the Galilee Basin. See also p125, p131 fig GLL12, p132, p134 fig GLL17, p135, p136, p141, p144, p305.||||Unconformably overlies the Jochmus Formation. Overlain by the Bandanna Formation.|Medium to coarse-grained quartzose sandstones interbedded with mudstones, siltstones and fine-grained tight sandstones.|
27129|Colinlea Sandstone|68279|5|Briefly described|p2, p4, p5 Tb.2, p7-9, p16 Tb.4, p18-19|Lopingian|Guadalupian|Galilee Basin. Fluvial unit. Significant concentration of pyrite suggests prolonged marine influence. Galilee Basin stratigraphic cross-sections, and mineralogy tables.||||Is overlain by Peawaddy Formation.|Light grey to brown, thick-bedded, fine- to coarse-grained, moderately to poorly sorted, sublabile to quartzose sandstone, conglomeratic in places; minor mudstone, siltstone and coal.|
27129|Colinlea Sandstone|68326|5|Briefly described|Map legend.|Permian|Permian|Galilee Basin.|||||Quartz sandstone, pebbly quartz sandstone, minor conglomerate and siltstone.|02-DEC-13
27129|Colinlea Sandstone|68411|5|Briefly described|Map Legend|Permian|Permian|Galilee Basin||Of the Back Creek Group.||Conformably underlain by the Reids Dome beds. Conformably overlain by the Peawaddy Formation.|Quartz sandstone, pebbly quartz sandstone, minor conglomerate and siltstone.|
27129|Colinlea Sandstone|68414|5|Briefly described|Map Legend|Permian|Permian|Bowen Basin.||Of the Back Creek Group.||Conformably overlain by the Peawaddy Formation. Underlain by the Joe Joe Goup.|Quartz sandstone, pebbly quartz sandstone, minor conglomerate and siltstone.|18-JUN-13
27129|Colinlea Sandstone|68423|5|Briefly described|map legend|Permian|Permian|Galilee Basin.|||||Quartz sandstone, pebbly quartz sandstone, minor conglomerate and siltstone.|
27129|Colinlea Sandstone|68679|5|Briefly described|p378, p380|||Mollan et al. (1969). Bowen, Galilee Basins. 200m thick. Fluvial plain, marginal marine deposits.|||||Sandstone, pebbly sandstone, conglomerate.|
27129|Colinlea Sandstone|68731|6|Mentioned|p201 Fig 3.110|Lopingian|Lopingian|Correlative of the upper Aldebaran Sandstone, Feitag Formation, Ingelara Formation and Catherine Sandstone.||||||
27129|Colinlea Sandstone|69379|5|Briefly described|map legend|Permian|Permian|||Of Back Creek Group|||Quartz sandstone, pebbly quartz sandstone, minor conglomerate and siltstone|
27129|Colinlea Sandstone|69582|6|Mentioned|p66|||Galilee Basin. Intersected in GSQ Longreach 2 drillhole.||||Overlies the Aramac Coal Measures. Overlain by the Bandanna Formation.|Sandstone.|
27129|Colinlea Sandstone|70857|5|Briefly described|Map Legend|Permian|Permian|||Back Creek Group||Overlain by Peawaddy Formation|Quartz sandstone, pebbly quartz sandstone, minor conglomerate and siltstone.|
27129|Colinlea Sandstone|71265|5|Briefly described|p587, p589-592, p595-600, p603-607|Changhsingian|Wuchiapingian|Galilee Basin. References to "Colinlea Sandstone equivalent" as previously Colinlea Sandstone. 40-70m thick. Sedimentary logs of GSQ Muttaburra 1, CRD Montani 1 and OEC Glue Pot Creek 1. Facies discussed.||||Overlies Jochmus Formation (Joe Joe Group). Is overlain by Fair Hill Formation and Fort Cooper Coal Measures. Interfingers with, and lateral equivalent of, Peawaddy Formation.|Dominated by quartz-rich sandstone. Contains a series of fining-upward sequences capped by coal.|
27129|Colinlea Sandstone|71276|4|Described|p284-286, p288-295, p297-298|Lopingian|Lopingian|Mollan et al. (1969). Formerly the Colinlea Formation of Schneeberger (1952). Type section on the Springsure Shelf. Similar basal conglomerate, sandstone composition, and palynology to Betts Creek beds, but separation of > 450km makes correlation questionable. Suggested (Mollan et al., 1969) as probable lateral equivalent of Aldebaran Sandstone, Ingelara Formation and Catherine Sandstone. Coal seam correlation. Proposed in this study that, within the Galilee Basin, this unit be given the informal name "Colinlea Sandstone equivalent" on the grounds that the original description is no longer appropriate.||||Is overlain by Peawaddy Formation. Correlative of Betts Creek beds.|Predominantly fine to medium quartz sandstone with a kaolinitic matrix. Basal conglomerate. Contains four coal seams.|
27129|Colinlea Sandstone|71701|5|Briefly described|p155-p158, p163, p166-p169|Changhsingian|Changhsingian|Eastern Area and Springsure Shelf, Galilee Basin. Palynology of an equivalent unit is discussed briefly. ||||Overlies the Joe Joe Group. Overlain by the Fair Hill Formation. Equivalent to the upper part of the Moranbah Coal Measures.||
27129|Colinlea Sandstone|71710|5|Briefly described|p367, 370, p380-381, p386|||Southern Galilee Basin. ||||Equivalent to lower part of Betts Creek beds. Disconformity at base.||
27129|Colinlea Sandstone|72088|5|Briefly described|p8, p16, p18, p20-p21|Wuchiapingian|Wuchiapingian|Southern Galilee Basin. See also p38-p40, p43-p44, p68-p69, p91.||||Overlain by the Peawaddy Formation and the Bandanna Formation.||
27129|Colinlea Sandstone|72297|5|Briefly described|p752-753, p755|Permian|Permian|Galilee Basin. 120m thick. Hosts the Alpha oil shale deposit (described).|||||Cross-bedded sandstone with minor conglomerate, siltstone, mudstone, coal and oil shale (torbanite).|
27129|Colinlea Sandstone|73163|5|Briefly described|p468|Lopingian|Lopingian|Springsure Shelf.||||Lateral equivalent of the Colinlea Sandstone equivalent.|Predominantly composed of quartz, lower part is feldspar-deficient, upper part contains more feldspar. Basal conglomerate contains chert, volcanic rocks, subordinate quartzite.|
27129|Colinlea Sandstone|73472|6|Mentioned|p115-116|Wuchiapingian|Capitanian|Galilee Basin.||||Overlain by Peawaddy Formation. Equivalent to Betts Creek beds, Catherine Sandstone, Ingelara Formation, Freitag Formation, and Aldebaran Sandstone.||
27129|Colinlea Sandstone|73625|6|Mentioned|p19|Permian|Permian|Western Bowen Basin. Contains low-diversity floras of glossopterid and cordaitalean gymnosperms.||||||
75386|Colona Gabbro|65390|6|Mentioned|p22 Fig. 3|Statherian|Statherian|Fowler Domain, Gawler Craton. Age of 1730 Ma given.||||||
75386|Colona Gabbro|71862|4|Described|p7, p11, p13-p14, p23, p30|Statherian|Statherian|Named for the Colona Homestead, northwestern South Australia 790428mE, 6487324mN, GDA94, Zone 52. This unit does not outcrop but is intersected in ~20 drillholes in the Colona Homestead area in the western Gawler Craton. The type locality is defined as diamond drillhole COL43D (DH number 137323, 771569mE, 6527778mN, GDA94, Zone 52 between 52-69m. This unit has been affected by amphibolite facies metamorphism and weak to strong tectonic fabrics. An additional magmatic crystallisation age of 1729 +/- 7 Ma is derived from Fanning et al, 2007. Magmatic age is estimated at c. 1735 Ma. See also p33-p36, p42, p59-p61.|1739 +/- 6 Ma (magmatic cry. Reid, 2015)|Pinbong Suite|||Layered intermediate to mafic intrusive rocks including granodiorite, tonalite and hornblende gabbros.|
77399|Colona metagabbro|65376|6|Mentioned|p121. |||Not a formal name. Fowler Domain, Gawler Craton. See p170 for sample description.|1727+/-8 Ma SHRIMP magmatic crystallisation|||||29-OCT-12
80216|Comet Bore Member|73162|5|Briefly described|p452, p453, p458|Mesoproterozoic|Mesoproterozoic|Roopena Basin. Deposited in southeast and northwest parts of the basin. Records episode of extra-basinal felsic volcanism synchronous with sedimentation of Fresh Well Formation. Uppermost of three tuff members in the upper Fresh Well Formation. ~6m thick.||Fresh Well Formation, upper||Interlayered with the upper Fresh Well Formation.|Well sorted and laminated tuff, composed of quartz and minor lithic felsic volcanic and sedimentary clasts, matrix of sericite and clay, sharp basal and sharp to gradational upper contacts, approximately 6 m thick.|
23499|Con Bore Granite|22631|6|Mentioned|p176|Calymmian|Calymmian|||||||
23499|Con Bore Granite|24197|5|Briefly described|p75 Tb. 8.1|Mesoproterozoic|Mesoproterozoic|Age: 1560Ma.||||||07-FEB-11
23499|Con Bore Granite|42885|2|Defined|p25||Mesoproterozoic|see also Fig.3 p24||||||12-NOV-14
23499|Con Bore Granite|43052|5|Briefly described|Table 5.12|||||||||
23499|Con Bore Granite|50605|5|Briefly described|p(iii), 1.4, 10.2, Table 1.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Gawler Craton & Curnamona Province. Of the Moolawatana Suite.||||||
23499|Con Bore Granite|68068|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Curnamona Province.||Unit in Moolawatana Suite.|||Mostly non-porphyritic, greyish, large volcanic xenoliths, partly granophyric, fine- to coarse-grained biotite granite; composed of quartz, K-feldspar, plagioclase and biotite with accessory fluorite, apatite, tourmaline, pyrite and chalcopyrite.|
23499|Con Bore Granite|69023|3|Fully described|p26, p35-37, p47-48, p50-51, p53-54|||See also p145, p189. Of Teale (1993); previously included in Mount Neill Granite Porphyry by Coats et al. (1969). Mount Painter Inlier. Type area is east of Mount Fitton. High level emplacement. Distinct geochemical signature described. Similar mineralogy to that of Golden Pole Granite. No radiometric age; presumed late Mesoproterozoic.||Unit in Moolawatana Suite.||Intrudes Terrapinna Granite. Is overlain unconformably by Fitton Formation.|A number of non-porphyritic variants from fine- to coarse-grained; volcanic to subvolcanic xenoliths common.|
23499|Con Bore Granite|70384|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic||||||Mostly non-porphyritic, greyish with large volcanic xenoliths, partly granophyric, fine- to coarse-grained biotite granite. Composed of quartz, K-feldspar, plagioclase and biotite; accessory fluorite, apatite, tourmaline, pyrite and chalcopyrite.|
39566|Cooalinga Member|24465|5|Briefly described|p353|Early Cambrian|Early Cambrian|Of Talisker Formation. Formerly Cooalinga Sandstone Member. Now includes rocks previously known as Malabena Sandstone Member.||||||
39566|Cooalinga Member|61046|5|Briefly described|p8 Fig. 2|Early Cambrian|Early Cambrian|Of Talisker Formation (Kanmantoo Group). Mount Torrens Pb-Ag prospect and Holmes Watson prospect within valley-fill in this member.||||||
39566|Cooalinga Member|63848|6|Mentioned|p534 Fig.4.|||||Unit in Talisker Formation.||||
39566|Cooalinga Member|65664|5|Briefly described|p1096, p1101 Tab.1, p1104-5, p1106 Fig.5|Early Cambrian|Early Cambrian|||Base of Talisker Formation.|||Sandy to conglomeratic. Deposited in a deep water turbiditic environment.|09-MAY-12
27375|Coober Pedy Paleosol|38604|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
27375|Coober Pedy Paleosol|38605|4|Described|p40|||||||||
27375|Coober Pedy Paleosol|42816|6|Mentioned|p27|||||||||
73492|Coodnambana Metaconglomerate|66302|6|Mentioned|p20, p32|||Mount Woods Domain, Gawler Craton. Metamorphic age of 1595 +/- 10 Ma (Jagodzinski et al, 2007; Chalmer 2007)|1749 +/- 6 Ma (maximum depositional age)|Mount Woods Complex||Unconformably overlies the Skylark Metasediments.||
73492|Coodnambana Metaconglomerate|67621|6|Mentioned|p211, 222|||Gawler Craton. Appears as Coonambana Conglomerate on p22. Unconformably overlies the Mount Woods Inlier.|||||Interbedded sandstones and conglomerates.|
73492|Coodnambana Metaconglomerate|73155|5|Briefly described|p265|||Mount Woods Domain. Exposed at Spire Hill. Clasts appear derived from Skylark Metasediments, with a minor population of clasts exotic to Gawler Craton. Ca. 1560 Ma monazite U-Pb age interpreted to date period of hydrothermal activity (O'Sullivan, 2010), consistent with Kararan Orogeny. See also Coodnambanna Metaconglomerate.||||Unconformably overlies Skylark Metasediments.|Interbedded sandstone and conglomerate.|
25712|Cook Gap Schist|22629|6|Mentioned|p149|Paleoproterozoic|Paleoproterozoic|part of Hutchison Group (Middleback Subgroup).||||||07-NOV-08
25712|Cook Gap Schist|23205|6|Mentioned|p42|||of Gawler Craton.||||||
25712|Cook Gap Schist|23285|5|Briefly described|Fig 3 p 333|||||||||
25712|Cook Gap Schist|23492|6|Mentioned|p6||Proterozoic|Equates with rocks that host graphite. Of Lower Middleback Subgroup/Hutchison Group.||||||
25712|Cook Gap Schist|23719|4|Described|p14|Statherian|Statherian|See also page 14 Table 1. Also known as Mangalo Schist. Age: 1688+/-76 Ma (Rb-Sr). Of Middleback Subgroup. Overlain by Upper Middleback Jaspilite. U'lying unit Lower Middleback Jaspilite. Geol. Prov: Gawler Craton. Max. thickness: >1500 m.||||||02-JUN-09
25712|Cook Gap Schist|23731|6|Mentioned|p21 Fig. 1.4|||||||||
25712|Cook Gap Schist|23791|5|Briefly described|p4|||Parent: Hutchinson Group.  Geological Province: Gawler Craton.||||||
25712|Cook Gap Schist|30806|5|Briefly described|p946|||||||||
25712|Cook Gap Schist|30845|6|Mentioned|p31|||||||||
25712|Cook Gap Schist|35298|5|Briefly described|p946|||||||||
25712|Cook Gap Schist|37811|1|Redefined|p237|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
25712|Cook Gap Schist|39345|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
25712|Cook Gap Schist|39349|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
25712|Cook Gap Schist|39353|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
25712|Cook Gap Schist|39802|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
25712|Cook Gap Schist|40227|6|Mentioned|Fig.2|||||||||
25712|Cook Gap Schist|40445|5|Briefly described|p47|||||||||
25712|Cook Gap Schist|40448|5|Briefly described|p30|||Also mention on Table 1.||||||
25712|Cook Gap Schist|40644|6|Mentioned|p124 Fig. 3, p132|Mesoproterozoic|Mesoproterozoic|Of the Middleback Subgroup (Hutchinson Group). Age: ~1688+/-76Ma.  See also the misspelt Cook Cap Schist.  See also Fig. 11.||||||13-AUG-08
25712|Cook Gap Schist|41325|6|Mentioned|Fig.2|||||||||
25712|Cook Gap Schist|41327|6|Mentioned|Fig.2|||||||||
25712|Cook Gap Schist|41619|6|Mentioned|Map legend|Paleoproterozoic||||||||07-NOV-08
25712|Cook Gap Schist|41667|6|Mentioned|p5|||See also p36.||||||16-MAR-21
25712|Cook Gap Schist|42738|5|Briefly described|map legend|Paleoproterozoic||Locally known as Mangalo Schist||||||07-NOV-08
25712|Cook Gap Schist|43052|5|Briefly described|p56|||of Middleback Subgroup||||||
25712|Cook Gap Schist|50605|5|Briefly described|p3.3|||Of the Hutchison Group. Geological Province: Gawler Craton & Curnamona Province.||||||
25712|Cook Gap Schist|61070|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Middleback Subgroup. Medium-grained biotite-sillimanite-rich quartzofeldspathic schist, grading to gneiss, with partial migmatisation in high-grade areas. Locally Sillimanite replaced by andalusite. Geological Province: Gawler Craton.||||||12-JAN-10
25712|Cook Gap Schist|62893|4|Described|Map Legend, p10-11, p13-14, p22, p36-38|Early Proterozoic|Early Proterozoic|Locally known as Mangalo Schist in the Cleve Uplands region. Ages of 1688 +/- 76 Ma (Rb-Sr) and younger from K-Ar dating reflect metamorphic overprinting. Grades from muscovite-bearing schist to sillimanite-bearing gneiss north of the Cleve Uplands. Well foliated, multiple deformed and concordant amphibolite bodies are common within the schist. Similar in outcrop appearance to the Yadnarie Schist, but with a lesser proportion of muscovite and amphibolite is absent.||Middleback Subgroup, Hutchison Group||Underlain by and interlayered with Lower Middleback Jaspilite, Katunga Dolomite, and Warrow Quartzite. Conformably overlain by Upper Middleback Jaspilite.|Well layered and well foliated, quartz-veined, semi-pelitic biotite-muscovite-garnet schist and gneiss, with local minor quartz-feldspar psammitic interbeds; local pegmatite sills and dykes.|
25712|Cook Gap Schist|65376|5|Briefly described|p54, pp60-61.|Paleoproterozoic|Paleoproterozoic||Detrital zircons aged c.1790 Ma.|Unit in Middleback Subgroup.||||
25712|Cook Gap Schist|65922|5|Briefly described|p14 Tb. 1, p15|Orosirian|Orosirian|Of Middleback Subgroup, Hutchison Group, Gawler Craton. Grey quartzofeldspathic gneiss to quartz-muscovite-biotite schist and local graphite schist. Strongly and often multiply foliated. Overlies Lower Middleback Jaspilite. Compositionally similar to Yadnarie Schist.||||||
25712|Cook Gap Schist|66302|6|Mentioned|p24|||||Middleback Subgroup||Overlies the Warrow Quartzite.||
25712|Cook Gap Schist|66882|4|Described|p101,p103 Fig.3a,b,c, p105-107,p109-112|Neoarchean|Neoarchean|See also p114-116, p118. Middleback Range. Outcrops to the W of the Kalinjala Mylonite Zone are now part of Mangalo Schist (Cleve Group). Appears as Cook gap schist on p105. No detrital zircons <2570 Ma; likely age c.2570 Ma. Other max. deposition ages are given (pp105-107) as 1843+/-10 Ma and 1784+/-17 Ma; these are not considered lateral equivalents. Isotope data. Geochemistry discussed. All Late Archean zircon peaks are present in Hamersley Group, suggesting correlation.|Max deposition 2566 +/- 20 Ma|Middleback Group||Underlies Upper Middleback Jaspilite, overlies Lower Middleback Jaspilite. Previously considered equivalent to Mangalo Schist.||02-MAR-15
25712|Cook Gap Schist|67721|4|Described|pp33-38|Archean|Archean|Type locality near Cook Gap, in the southern Middleback Range. Minimum detrital zircon peak occurs at 2570 Ma. Between 0-220/300 m thick. |< c. 3150 Ma|Of the Middleback Group.|Now including Long Gully member?|Conformably underlain by the Lower Middleback Jaspilite.|Comprises a typical mineral assemblage of quartz + feldspar + biotite + chlorite +/- garnet and varies in lithology from pelitic to semi-pelitic schist, exhibiting a prominent, subvertical crenulation clevage.|27-FEB-15
25712|Cook Gap Schist|68131|4|Described|p3 Tb.1, p5, p57-p66|Paleoproterozoic|Paleoproterozoic|The type section is in the Southern Middleback Ranges. Placed in inverted commas on p5 and p57. The dated sample may be from  a younger schist sequence e.g. Broadview Schist equivalent.|1796 +/- 6 Ma (maximum depositional age).|Middleback Subgroup.||Overlies Lower Middleback Jaspilite. Is overlain by Upper Middleback Jaspilite.|Schist.|15-MAR-21
25712|Cook Gap Schist|68208|6|Mentioned|p33|Paleoproterozoic|Paleoproterozoic|Contains a large 3150 Ma detrital zircon component. Some uncertainty regarding depositional age, which could be as old as Neoarchean based on the work of Szpunar et al. 2011.||Of Middleback Group||||
25712|Cook Gap Schist|71235|6|Mentioned|p9|||||Hutchison Group||||
25712|Cook Gap Schist|71536|5|Briefly described|p79, p88|||Correlated with the youngest rock (a mica-rich schist) in the Wilgerup sequence.||||Overlies the Lower Middleback Jaspilite.||
25712|Cook Gap Schist|71859|6|Mentioned|p18|||||Hutchison Group||||
25712|Cook Gap Schist|72058|6|Mentioned|p171-p172, p190, p192|||Middleback Ranges, Gawler Craton.|~2565 Ma|Middleback Group||Overlies the Lower Middleback Iron Formation. Overlain by the Upper Middleback Iron Formation.||16-MAR-21
25712|Cook Gap Schist|72484|5|Briefly described|p2-3, 5, 6-7 Tbls 1A-1B, 13-16 Tbls 2-3|||Eyre Peninsula, Gawler Craton. Whole-rock and trace element geochemistry tabulated. This MDA was determined  by SHRIMP U-Pb zircon. Ages of older groups of zircons in this unit, and their likely sources, are discussed. See also p18, 20-21, 23-24.|2585 +/- 22 Ma (MDA).|Middleback Subgroup.||Gradationally overlies Lower Middleback Iron Formation. Is overlain gradationally by Upper Middleback Iron Formation.|Green, medium-grained quartz-amphibolite schist; a marker horizon comprising garnet-bearing mica schists.|
25712|Cook Gap Schist|73103|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic||||||Schist, medium-grained, biotite-garnet-sillimanite quartzo-feldspathic, grading to gneiss, migmatised in high-grade area, locally graphitic.|
25712|Cook Gap Schist|73110|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|The Legend mentions this unit thus: Amphibolite. Based on Prot-beta as portrayed on WHYALLA, but only where not associated with Cook Gap/Mangalo Schist or Broadview Schist.||||||
23505|Coolanie Gneiss|22849|5|Briefly described|20|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
23505|Coolanie Gneiss|23719|4|Described|p21|Paleoproterozoic|Paleoproterozoic|See also page 19 table 5. Geological Province: Gawler Craton.||||||07-NOV-08
23505|Coolanie Gneiss|39349|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
23505|Coolanie Gneiss|39353|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
23505|Coolanie Gneiss|40227|6|Mentioned|p44|||||||||
23505|Coolanie Gneiss|41667|4|Described|p66|||||||||
23505|Coolanie Gneiss|43052|5|Briefly described|p74|||||||||
23505|Coolanie Gneiss|66302|6|Mentioned|p14|Neoarchean|Mesoarchean|Igneous crystallisation age; a metamorphic SHRIMP age of 2427 +/- 5 Ma is also given. |2823 +/- 37 Ma (Fraser and Neumann 2010)|||||
23505|Coolanie Gneiss|68208|6|Mentioned|p32|||Part of what was previously known as the Narridy Creek granite.||||||
23505|Coolanie Gneiss|69048|6|Mentioned|p3|||Central-western Eyre Peninsula.||||||
23505|Coolanie Gneiss|70721|6|Mentioned|p63, p73||||c. 2820 Ma|||||
23505|Coolanie Gneiss|71037|6|Mentioned|p21 Fig.1|Archean|Archean|Shown only on 'Outcropping geology and mineral deposits of northern Eyre Peninsula' map p21 Fig.1. These Archean rocks are shown in the southeastern part of the Eyre Peninsular.||||Shown as younger than Cooyerdoo Granite and older than Sleaford Complex.|Gneiss.|
23505|Coolanie Gneiss|71129|6|Mentioned|p14,17-18,23,203|Mesoarchean|Mesoarchean|Geological Province: Cleve-Coulta Domain, Gawler Craton.||||Overlain by the Sleaford Complex.||13-NOV-19
23505|Coolanie Gneiss|71317|5|Briefly described|p14, p16|Mesoarchean|Mesoarchean|Cleve-Coulta Domains, Gawler Craton.|c. 2820 Ma (Fraser et al., 2010)|||||
23505|Coolanie Gneiss|71559|6|Mentioned|p15 Fig 1|Archean|Archean|Geological province: Gawler Craton.||||||
23505|Coolanie Gneiss|71859|4|Described|p1-p4, p6, p14, p18, p24, p28, p35|Mesoarchean|Mesoarchean|Southern Gawler Craton, Cleve and Coulta Domains. Crops out as a linear belt adjacent to the Minbrie Gneiss. Derived from remelting of a source region similar to the Minbrie Gneiss. Forms basement in the southern Gawler Craton. Outcrops on the northeastern Eyre Peninsula. In contact with the Carpa Granite. Has an inferred structural contact with the Minbrie Gneiss.|c. 2820 Ma|||Overlain by the Sleaford and Mulgathing complexes.|S-type Granite.|04-APR-23
23505|Coolanie Gneiss|71862|5|Briefly described|p2-p4, p8, p12|||Originally a part of the now obsolete Lincoln Complex.|c. 2820 Ma|||||12-APR-23
23505|Coolanie Gneiss|72090|6|Mentioned|p10|Archean|Archean|Cleve-Coulta Domain, Gawler Craton.|c. 2620 Ma|||||
23505|Coolanie Gneiss|72462|6|Mentioned|p3|Archean|Archean|Gawler Craton.||||||
23505|Coolanie Gneiss|72484|5|Briefly described|p2, 22|||Gneissic basement formed by amphibolite to granulite facies metamorphism of the Sleafordian Orogeny. The protolith to this unit was emplaced at 2823 +/- 37 Ma (zircon: Fraser et al., 2010).|~2.47-2.41 Ga.|||||
23505|Coolanie Gneiss|73026|5|Briefly described|p5-6|Neoarchean|Neoarchean|Central/western Eyre Peninsula. The protolith to this unit forms the oldest component of the Mulgathing and Sleaford Complexes.|2823 +/- 37 (protolith, Fraser and Neumann, 2010)||||Gneiss.|
23505|Coolanie Gneiss|73027|6|Mentioned|p4|Palaeoproterozoic|Palaeoproterozoic||2823 +/- 37 Ma (emplacement age)|||||
23505|Coolanie Gneiss|73103|5|Briefly described|Map legend.|Archean|Archean|Metamorphosed at 2427 +/- 4 Ma.|2823 +/- 37 Ma (crystallisation).||||Gneiss, mylonitic and augen; granite gneiss, often fine-grained, strongly rodded.|
23505|Coolanie Gneiss|73130|6|Mentioned|[poster]|Mesoarchean|Mesoarchean|Constitutes basement beneath the Itiledoo Basin.|c. 2820 Ma|||||
23505|Coolanie Gneiss|73165|6|Mentioned|p621|Mesoarchean|Mesoarchean|Gawler Craton. Associated with felsic magmatism.|ca 2823 Ma|||||
24225|Coolardie Formation|37851|2|Defined|p9|Permian|Carboniferous|Permo-Carboniferous||||||
24225|Coolardie Formation|40448|4|Described|p41|||||||||
24225|Coolardie Formation|40673|6|Mentioned|p12|||||||||
24225|Coolardie Formation|41218|6|Mentioned|p329|||||||||
24225|Coolardie Formation|41363|6|Mentioned|p16|||||||||
24225|Coolardie Formation|42716|5|Briefly described|Map legend|Permian|Carboniferous|||||||
24225|Coolardie Formation|42738|5|Briefly described|map legend|Permian|Carboniferous|||||||
24225|Coolardie Formation|43049|4|Described|p21|||||||||
24225|Coolardie Formation|43052|5|Briefly described|p202|||||||||
24225|Coolardie Formation|43671|5|Briefly described|p4|Permian|Carboniferous|||||||
24225|Coolardie Formation|44133|4|Described|p65 Fig. 8.4, 72 Fig. 8.11|Permian|Carboniferous|Geological Province: Polda Basin. Type section 181m thick. Unconformably overlies Kilroo Formation. Unconformably overlain by Polda Formation.||||||
24225|Coolardie Formation|62893|4|Described|Map Legend, p18-19, p29|Permian|Carboniferous|Polda Basin (subsurface). Glacial-marine. Matrix-supported conglomerate is common towards the top. Type section is in SADME Lock 1 drillhole where the unit is 181 m thick. Only fully penetrated (within Kimba mapsheet area) by CRA 83 KD 1A with a thickness of 22 m [where it contains] two lithotypes; a basal 12 m thick succession of dark grey, matrix-supported massive diamictite with angular to subrounded pebbles, and an upper 10 m thick succession of white, well sorted, fine-grained, thinly bedded sandstone with minor pebble and diamictite bands. Topmost 9 m represents an intensely kaolinised weathering profile.||||Unconformably underlain by Kilroo Formation. Unconformably overlain by Polda Formation. Equivalent to Cape Jervis Formation, Boorthanna Formation, and Stuart Range Formation.|Brown, grey, green and white diamictite, pebbly mudstone, siltstone and sandstone.|
26491|Coomb Spring Formation|23155|6|Mentioned|p37|||From the FROME and CURNAMONA map sheets.||||||
26491|Coomb Spring Formation|39804|6|Mentioned|p173|||Correct spelling of Coombes||||||
26491|Coomb Spring Formation|40914|6|Mentioned|Map legend|Cenozoic|Cenozoic|||||||19-NOV-08
26491|Coomb Spring Formation|42090|3|Fully described|p38|||||||||
26491|Coomb Spring Formation|42592|6|Mentioned|p280|||||||||
26491|Coomb Spring Formation|42746|5|Briefly described|p22|||||||||
26491|Coomb Spring Formation|42784|6|Mentioned|p494|||||||||
26491|Coomb Spring Formation|44133|5|Briefly described|p247, 244 Table 11.3|Late Pleistocene|Middle Pleistocene|Maximum Thickness: 8m. ||||||
26491|Coomb Spring Formation|60953|5|Briefly described|Map Legend|Pleistocene|Pleistocene|Fine to coarse fossiliferous sand and gravel.||||||
26491|Coomb Spring Formation|61108|5|Briefly described|map legend|Pleistocene|Pleistocene|Lacustrine strandline sediments: fine to coarse fossiliferous sand and gravel.||||||
26491|Coomb Spring Formation|65925|5|Briefly described|pp17-18.|Pleistocene|Pleistocene|Beach deposits around Lake Frome. Up to 8m thick.||||Intertongues with Millyera Formation.|White to yellow, often coarse-grained, well-sorted sand.|
26491|Coomb Spring Formation|66131|6|Mentioned|p240, p247|Pleistocene|Pleistocene|Age may extend back to 140 ka.||||Intertongues with Millyera Formation.|Beach sand (representing higher levels of Lake Frome).|
26491|Coomb Spring Formation|68068|5|Briefly described|Map legend|Pleistocene|Pleistocene|Callabonna Sub-basin, Lake Eyre Basin. Forms strand ridge lines marking palaeo- and modern high water stands to Lakes Blanche and Callabonna. In part equivalent to Millyera Formation.|26.2 +/- 3.0 ky (TL) to present.|||Overlies Millyera Formation.|Beach facies gravel and sand; intense red-brown to greenish-yellow to pale grey; usually uncemented, ranges from loose to consolidated; may contain fish bones, mollusc shells, ostracods, wood and algal remains.|
26491|Coomb Spring Formation|69019|5|Briefly described|p106 Fig.26, p120-121.|Pleistocene|Pleistocene|Of Callen (1990). W of Lake Blanche. Mis-spelt as Coombe in Fig.26. Beach facies equivalent to Millyera Formation. Age-dating discussed.|54.9 +/- 4.8 ka to 22.1 +/- 4 ka BP.||||Sandy to gravelly near shore and beach deposits, commonly as a series of strand lines.|09-JUN-22
26491|Coomb Spring Formation|69023|5|Briefly described|p109, p126-127, p133-134, p142|Pleistocene|Pleistocene|Defined in Callen (1990). Appears in Fig.25 as Coombe [sic] Spring & Millyera Formation. Represents nearshore and beach facies of paleo-lakes in alternating dry and wet intervals in Quaternary SA. Originally defined in Lake Frome area; subsequently extended N and NW. Diverse fossils listed. Age discussed in some detail.|||||Sandy to gravelly deposits, commonly as a series of strand lines; greenish-yellow to white, grading to intense red-brown, sand with abundant fish bones, gastropods, ostracods and algae; concentric gravel beach ridges are unfossiliferous.|
26491|Coomb Spring Formation|72456|5|Briefly described|Map Legend|Pleistocene|Pleistocene|Marree 1:250k map sheet. Deposited in a lacustrine or beach ridge environment.|||||Sand, white to yellow, coarse-grained, well sorted.|
26491|Coomb Spring Formation|72457|6|Mentioned|p91|Pleistocene|Pleistocene|Callabonna Sub-basin. Shoreline deposits.||||||
24226|Coominaree Dolomite|22589|6|Mentioned|p129,30|Cryogenian||||||||
24226|Coominaree Dolomite|22922|5|Briefly described|32|||||||||
24226|Coominaree Dolomite|23054|5|Briefly described|p10|||||||||
24226|Coominaree Dolomite|23282|2|Defined|p52||Neoproterozoic|Age: Precambrian, Neoproterozoic, Willouran to Torrensian Epochs. of Ambrose et al (1981). Lateral facies equiv. of the upper Alinya Formation and may correlate with the Skates Hill Formation. Stromatolite fossil assemblage present.||||||24-MAR-21
24226|Coominaree Dolomite|23288|6|Mentioned|p128 Fig.5,18|||of Central and Eastern Officer Basin.||||||
24226|Coominaree Dolomite|23314|5|Briefly described|331 Fig.2|||||||||
24226|Coominaree Dolomite|23557|5|Briefly described|p98|Cryogenian|Cryogenian|Geological Province: Adelaide Rift Complex.||||||
24226|Coominaree Dolomite|24112|5|Briefly described|p254 Fig.2|Neoproterozoic|Neoproterozoic|Of the Callanna Group. Geological Province: Officer Basin||||||
24226|Coominaree Dolomite|36733|2|Defined|p68|early Adelaidean|early Adelaidean|See also p24.||||||29-AUG-18
24226|Coominaree Dolomite|37854|6|Mentioned|p9|||||||||
24226|Coominaree Dolomite|38108|6|Mentioned|Table 1|||||||||
24226|Coominaree Dolomite|38157|6|Mentioned|Table II|||||||||
24226|Coominaree Dolomite|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Willouran||||||
24226|Coominaree Dolomite|39490|6|Mentioned|p10|||||||||
24226|Coominaree Dolomite|40294|6|Mentioned|p8|||See also Table 2||||||
24226|Coominaree Dolomite|41403|4|Described|p51|||||||||
24226|Coominaree Dolomite|42222|5|Briefly described|p11|||||||||
24226|Coominaree Dolomite|42223|6|Mentioned|Fig.2 P36|||||||||
24226|Coominaree Dolomite|43052|5|Briefly described|p172,Table 6.2|||of Arkaroola Subgroup||||||
24226|Coominaree Dolomite|43743|6|Mentioned|Fig.2,p33||Neoproterozoic|||||||
24226|Coominaree Dolomite|44111|6|Mentioned|p.58 Fig. 2|||in Adelaide Geosyncline. Fig.2 legend shows it as being volcanic rocks(?)||||||
24226|Coominaree Dolomite|44289|5|Briefly described|Map Legend||Neoproterozoic|||||||
24226|Coominaree Dolomite|62453|4|Described|p5 Fig. 3, 13, 24|Cryogenian|Cryogenian|Geological Province: Officer Basin. Siltstone, mudstone, sandstone, dolomite, minor evaporites. Underlies Rook Tuff.||||||
24226|Coominaree Dolomite|63397|6|Mentioned|5|||||||||
24226|Coominaree Dolomite|64793|5|Briefly described|p284 fig 3, p285 fig 4, p292|||Hosts Acaciella australica Stromatolite Assemblage.||Unit in Arkaroola Subgroup.||||
24226|Coominaree Dolomite|64796|5|Briefly described|p183 fig 2, p185, p187, p189 Fig.7 |Cryogenian|Cryogenian|See also p190 Fig.8, p193 Tb.1, p195 Tb.3, p199-201. Of Adelaide Rift Complex.|~830 Ma.|Unit in Arkaroola Subgroup.||Overlies Younghusband Conglomerate.|Stromatolitic dolomite.|
24226|Coominaree Dolomite|64797|6|Mentioned|p160 Fig.8|||||||||
24226|Coominaree Dolomite|65363|6|Mentioned|p11.|||Presence of Acaciella australica Stromatolite Assemblage in the Woolnough Member of the Browne Formation enables correlation with this unit, Skates Hill Formation, Loves Creek Member of the Bitter Springs Formation, and Yackah beds.||||||
24226|Coominaree Dolomite|65365|5|Briefly described|p1, 5, p6 Fig. 2, p10 Fig. 4|Cryogenian|Cryogenian|Peake and Denison Ranges, northern Adelaide Rift Complex. Minimum depositional age from intrusion by Gairdner Dyke Swarm (827 +/- 6 Ma). Includes stromatolite assemblages.||||||19-MAR-12
24226|Coominaree Dolomite|65366|5|Briefly described|p23 Fig. 3, p24|Cryogenian|Cryogenian|Of Arkaroola Subgroup, Callanna Group. Northern Adelaide Rift Complex. Includes the Acaciella australica Stromatolite Assemblage||||Underlies the Rook Tuff.||19-MAR-12
24226|Coominaree Dolomite|65454|6|Mentioned|p11|||Of Adelaide Rift Complex. Temporally correlated with Skates Hill Formation.||||||
24226|Coominaree Dolomite|69003|6|Mentioned|p60|Neoproterozoic|Neoproterozoic|E Officer Basin.||||||
24226|Coominaree Dolomite|69438|5|Briefly described|p23:11|||Adelaide Fold Belt.||Callanna Group.||Is correlated with the Bitter Springs Formation (Amadeus Basin).||12-JUL-16
24226|Coominaree Dolomite|72478|6|Mentioned|p8|Willouran|Torrensian|Officer Basin.|c. 790 Ma|Callanna Group||Overlies the Alinya Formation. Overlain by the Cadlareena Volcanics.||24-MAR-21
24226|Coominaree Dolomite|73086|6|Mentioned|p15, p18, p30, p148|||Adelaide Rift Complex. Correlation with Bitter Springs groups is based on isotopic and other geochemical studies.||||May correlate to Bitter Springs Group [and Browne Formation?].||
80193|Coompana Granite|70893|6|Mentioned|p92|||Samples R2132968,  R2132936 reported as being on same mount as 3 St Peter Suite samples, that were further described in this reference.||||||05-OCT-17
78977|Coompana Suite|69648|5|Briefly described|p16|Neoproterozoic||Rankin (2003), after informal Coompana Intrusives of Teasdale et al. (2001). Mafic dyke swarms. The most obvious and extensive dyke swarms within OOLDEA are NNW-trending negatively magnetic mafic dykes now thought to be associated with "Coompana Suite" of Rankin (2003). Western Gawler Craton. Considered older than the Gairdner Dyke Swarm.|||||Magnetic mafic dykes.|15-JAN-15
33822|Coongie Limestone Member|63056|5|Briefly described|p79, p81 Fig. 2|Early Cambrian|Early Cambrian|Characterised by several stacked cycles of carbonates. Thickness: ~550m. Geological Province: Warburton Basin. Shelf carbonate prograding into basin; good reservoir quality.||||||03-JUL-14
33822|Coongie Limestone Member|65489|5|Briefly described|p39, p96, p120|Late Cambrian|Middle Cambrian|Eastern Warburton Basin. Good reservoir quality.||Unit in Kalladeina Formation.||||
33822|Coongie Limestone Member|68731|6|Mentioned|p170 Fig 3.83|Middle Cambrian|Middle Cambrian|Shelf carbonate prograding into basin, good reservoir quality. ~ 550 m thick.||||||
33822|Coongie Limestone Member|69982|3|Fully described|p21-22, p45, p54, p70-71|Late Cambrian|Middle Cambrian|New informal name. Separated because of its distinct lithologies and importance as a potential carbonate reservoir. Type section is in Coongie 1 well, over the interval 3048 - 3605 m. Wireline log and simplified lithologies detailed. Peritidal carbonate deposit. Age from trilobites. Appears as Coongie Limestone on p42, p70-71. Porosity/permeability data. Brief thin section descriptions.||Unit in Kalladeina Formation.|||A thick limestone and dolomite dominated succession.|
33822|Coongie Limestone Member|73244|6|Mentioned|p86|Cambrian|Cambrian|Warburton Basin. Shallow shelf environment. Gas.||||||
33822|Coongie Limestone Member|73479|6|Mentioned|p156|Cambrian|Cambrian|Warburton Basin. Shallow shelf depositional environment.|ca 505-497 Ma|Kalladeina Formation||||
24227|Cooranna Formation|24175|3|Fully described|p10|Neoproterozoic|Neoproterozoic|Of Curdimurka Subgroup.  Overlies Hogan Dolomite; underlies Boorloo Siltstone.  Max. thickness: 781m.||||||
24227|Cooranna Formation|24321|5|Briefly described|Map legend|Adelaidean|Adelaidean|Parent: Curdimurka Subgroup||||||
24227|Cooranna Formation|37854|2|Defined|p12|Adelaidean|Adelaidean|Prob.Late Willouran||||||
24227|Cooranna Formation|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Willouran||||||
24227|Cooranna Formation|40294|6|Mentioned|p9|||||||||
24227|Cooranna Formation|41402|6|Mentioned|p42|||||||||
24227|Cooranna Formation|41403|4|Described|p65|||||||||
24227|Cooranna Formation|42222|5|Briefly described|p12|||||||||
24227|Cooranna Formation|42238|5|Briefly described|p78|||||||||
24227|Cooranna Formation|43052|5|Briefly described|p175,Table 6.1|||of Curdimurka Subgroup.||||||
24227|Cooranna Formation|60718|5|Briefly described|p49 Fig. 2, p52|Adelaidean|Adelaidean|Geological Province: Adelaide Geosyncline.||Of Curdimurka Subgroup (Callanna Group).||||15-APR-11
24227|Cooranna Formation|64796|6|Mentioned|p190 Fig.8, p194 Tb.2, p200 Fig.10|Neoproterozoic|Neoproterozoic|||Unit in Curdimurka Subgroup.||Overlies Hogan Dolomite. Is overlain by Boorloo Siltstone.||
24227|Cooranna Formation|64797|6|Mentioned|p161 Tb.4|||Adelaide Rift Complex. Lithology/rank not shown on diagram. S-isotope data. ||||||
24227|Cooranna Formation|69019|4|Described|p37.|Neoproterozoic|Neoproterozoic|Defined by Murrell (1977) with 4 un-named members. Type section is 2 km WSW of the Boorloo Mine where it is 781 m thick.||Unit in Curdimurka Subgroup.|||Greyish sandstone and siltstone with several sedimentary structures, variably pyritic; dolomite and limestone beds, more common in lower half; minor dark chert, gypsum, halite.|
24227|Cooranna Formation|72456|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Marree 1:250k map sheet. |||||Sandstone; siltstone, halite clasts, mudcracks, ripples.|
24227|Cooranna Formation|72492|4|Described|p2 Fig.1, p3, p5 Fig.4a, p5 Fig.4i|Neoproterozoic|Neoproterozoic|In the Willouran Ranges. Misspelt on p7 Tb.1 as 'Cooranna formation'. See also p7 Tb.1, p10 Tb.2, p11 Tb.3, p16.||Curdimurka Subgroup||Overlies Hogan Dolomite and underlies Boorloo Siltstone. Possibly correlated with Arkaba Hill beds.|Includes stromatolites, halite casts and desiccation cracks.|
24227|Cooranna Formation|73222|6|Mentioned|p7|Tonian|Tonian|Willouran Ranges. Torrensian.||Curdimurka Subgroup, Callanna Group, Warrina Supergroup||Underlain by Hogan Dolomite. Overlain by Boorloo Siltstone. Equivalent to Arkaba Hill Beds.||
24227|Cooranna Formation|74367|6|Mentioned|p7 Fig.6|||||Curdimurka Subgroup||||
26493|Coorikiana Sandstone|13497|5|Briefly described|p115 fig 6.33, p170, p171|Early Cretaceous|Early Cretaceous|Eromanga Basin. Sandstone were deposited in a shoreface environment. ||Marree Subgroup||Overlies the Bulldog Shale. Overlain by the Oodnadatta Formation.|Sandstone.|
26493|Coorikiana Sandstone|13516|6|Mentioned|p167 fig 10, p171 fig 12|Albian|Albian|In Eromanga Basin.||Of Marree Subgroup||||
26493|Coorikiana Sandstone|22874|6|Mentioned|P18|||||||||
26493|Coorikiana Sandstone|22883|5|Briefly described|Fig2 P30||Early Cretaceous|Overlying unit is Oodnadatta Formation, underlying unit is Bulldog Shale||||||
26493|Coorikiana Sandstone|22912|5|Briefly described|33|||Geol province Eromanga Basin||||||
26493|Coorikiana Sandstone|23054|5|Briefly described|p21,26,36||Albian|||||||
26493|Coorikiana Sandstone|23056|6|Mentioned|12 table 2|||||||||
26493|Coorikiana Sandstone|23154|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|Geological Province - Eromanga Basin.  Of the Marree Subgroup (Neales River Group).||||||21-MAY-08
26493|Coorikiana Sandstone|23155|4|Described|p30|Early Cretaceous|Early Cretaceous|Age - Aptian ?(text)     or     Albian ? (diagram)||||||
26493|Coorikiana Sandstone|23375|4|Described|Fig2 p265||Albian|In the Eromanga Basin.||||||21-MAY-08
26493|Coorikiana Sandstone|23982|5|Briefly described|p58 Fig.18|||Of Neales River Group. Geological Province: Eromanga Basin.||||||
26493|Coorikiana Sandstone|24092|5|Briefly described|p8 Fig.3|||Of Neales River Group. Geological Province: Eromanga Basin.||||||
26493|Coorikiana Sandstone|24175|3|Fully described|p26, p17 Fig. 3|Albian|Albian|Of Marree Group. Conformably overlain by Oodnadatta Sandstone;  transitionally overlies Bulldog Shale.  Max. thickness: 15m.  Geological Province: Eromanga Basin.||||||31-MAR-09
26493|Coorikiana Sandstone|24210|5|Briefly described|p133 Fig. 2|Early Cretaceous|Early Cretaceous|Of the Marree Subgroup.  Geological Province: Eromanga Basin.||||||
26493|Coorikiana Sandstone|24321|5|Briefly described|Map legend|Albian|Albian|Of the Marree Subgroup.||||||21-MAY-08
26493|Coorikiana Sandstone|30804|6|Mentioned|p10|||||||||
26493|Coorikiana Sandstone|33819|6|Mentioned|p1|||Cretaceous||||||
26493|Coorikiana Sandstone|33822|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
26493|Coorikiana Sandstone|33825|6|Mentioned|p10|||Correlation table||||||
26493|Coorikiana Sandstone|33827|6|Mentioned|p13|||||||||
26493|Coorikiana Sandstone|35002|6|Mentioned|p27|||||||||
26493|Coorikiana Sandstone|38730|6|Mentioned|p29|||||||||
26493|Coorikiana Sandstone|39352|6|Mentioned|Map legend|Albian|Aptian|Aptian to Albian||||||
26493|Coorikiana Sandstone|39914|6|Mentioned|p3|||||||||
26493|Coorikiana Sandstone|40003|5|Briefly described|Table 15|||||||||
26493|Coorikiana Sandstone|40058|6|Mentioned|p5|||||||||
26493|Coorikiana Sandstone|40199|6|Mentioned|p16|||See also Fig.1||||||
26493|Coorikiana Sandstone|40220|6|Mentioned|Fig.2|||||||||
26493|Coorikiana Sandstone|40670|6|Mentioned|Fig.9|||||||||
26493|Coorikiana Sandstone|40681|6|Mentioned|Fig.2|||||||||
26493|Coorikiana Sandstone|40910|6|Mentioned|p15|||||||||
26493|Coorikiana Sandstone|40911|6|Mentioned|Map legend|Cenomanian|Cenomanian|Prob. Cenomanian||||||
26493|Coorikiana Sandstone|40925|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
26493|Coorikiana Sandstone|40926|6|Mentioned|p17|||||||||
26493|Coorikiana Sandstone|41060|6|Mentioned|p2|||Generalized stratigraphy. See also Fig.3||||||
26493|Coorikiana Sandstone|41061|6|Mentioned|p9|||||||||
26493|Coorikiana Sandstone|41062|6|Mentioned|Fig.5|||||||||
26493|Coorikiana Sandstone|41064|6|Mentioned|p62|||||||||
26493|Coorikiana Sandstone|41084|5|Briefly described|Fig.2|||||||||
26493|Coorikiana Sandstone|41086|3|Fully described|p98|||||||||
26493|Coorikiana Sandstone|41087|6|Mentioned|Fig.2|||||||||
26493|Coorikiana Sandstone|41088|6|Mentioned|p143|||||||||
26493|Coorikiana Sandstone|41117|6|Mentioned|Fig.2|||||||||
26493|Coorikiana Sandstone|41165|5|Briefly described|p362|||See also Fig.15||||||
26493|Coorikiana Sandstone|41175|6|Mentioned|Fig.1|||||||||
26493|Coorikiana Sandstone|41177|6|Mentioned|Fig.2|||||||||
26493|Coorikiana Sandstone|41182|6|Mentioned|p287|||||||||
26493|Coorikiana Sandstone|41183|6|Mentioned|p307|||||||||
26493|Coorikiana Sandstone|41184|6|Mentioned|p328|||||||||
26493|Coorikiana Sandstone|41187|6|Mentioned|Fig.2|||||||||
26493|Coorikiana Sandstone|41216|6|Mentioned|Fig.18|||||||||
26493|Coorikiana Sandstone|41266|6|Mentioned|Fig.3|||||||||
26493|Coorikiana Sandstone|41523|3|Fully described|p276|||||||||
26493|Coorikiana Sandstone|41535|6|Mentioned|p368|||||||||
26493|Coorikiana Sandstone|41724|6|Mentioned|p383|||||||||
26493|Coorikiana Sandstone|41950|5|Briefly described|Fig.2 P3|||||||||
26493|Coorikiana Sandstone|42071|6|Mentioned|Table 2 P120|||||||||
26493|Coorikiana Sandstone|42085|6|Mentioned|Fig.2 P374|||||||||
26493|Coorikiana Sandstone|42293|6|Mentioned|Fig.2 P.18|||||||||
26493|Coorikiana Sandstone|42375|5|Briefly described|Fig.27 P122|Late Cretaceous|Jurassic|Eromanga Basin||||||
26493|Coorikiana Sandstone|42395|5|Briefly described|Fig.13 P83|||||||||
26493|Coorikiana Sandstone|42429|5|Briefly described|p155|||||||||
26493|Coorikiana Sandstone|42520|6|Mentioned|p6|||||||||
26493|Coorikiana Sandstone|42673|6|Mentioned|Fig.5 P189|||||||||
26493|Coorikiana Sandstone|42746|4|Described|p12|||See also Fig.6.||||||21-MAY-08
26493|Coorikiana Sandstone|43053|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Marginal marine sandstone and mudstone.||||||25-MAY-05
26493|Coorikiana Sandstone|43258|5|Briefly described|Map Legend||Cretaceous|||||||
26493|Coorikiana Sandstone|43298|5|Briefly described|Map Legend||Cretaceous|||||||
26493|Coorikiana Sandstone|43591|6|Mentioned|p176|||||||||
26493|Coorikiana Sandstone|43628|6|Mentioned|Fig.3||Early Cretaceous|||||||
26493|Coorikiana Sandstone|43681|5|Briefly described|p296|||||||||
26493|Coorikiana Sandstone|43711|6|Mentioned|p20|||||||||
26493|Coorikiana Sandstone|44133|4|Described|p120-121, 104 Fig 9.11, 117|Late Albian|Middle Albian|Geological Province: Eromanga Basin. Conformably overlies: Bulldog Shale. Formerly a member of the Oodnadatta Formation. Formerly named Attraction Hill Sandstone Member of the Marree Formation. ||||||
26493|Coorikiana Sandstone|44289|5|Briefly described|Map Legend||Albian|||||||
26493|Coorikiana Sandstone|60717|5|Briefly described|p40 Fig. 2|Early Cretaceous|Early Cretaceous|Overlies Bulldog Shale. Overlain by Oodnadatta Formation. Lateral to Toolebuc Formation and Allaru Mudstone; interfingers laterally with Mackunda Formation. Geological Province: Eromanga  Basin.||||||31-JAN-08
26493|Coorikiana Sandstone|60953|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Marginal marine sandstone and mudstone.||||||
26493|Coorikiana Sandstone|61108|5|Briefly described|map legend|Cretaceous|Cretaceous|Marginal marine sandstone and mudstone.||||||
26493|Coorikiana Sandstone|61312|5|Briefly described|p78, p79 Table E2|Cretaceous|Cretaceous|Of the Wallumbilla Formation (Rolling Downs Group). Geological Province: Eromanga Basin.||||||
26493|Coorikiana Sandstone|61613|6|Mentioned|p282 Fig. 2|Early Cretaceous|Early Cretaceous|Of Maree Subgroup. Geological Province: Eromanga Basin.||||||07-FEB-11
26493|Coorikiana Sandstone|61615|6|Mentioned|p302 Fig. 2|Early Cretaceous|Early Cretaceous|Of Marree Subgroup. Geological Province: Eromanga Basin.||||||07-FEB-11
26493|Coorikiana Sandstone|62029|5|Briefly described|p15 Fig. 4|Cretaceous|Cretaceous|||||||
26493|Coorikiana Sandstone|63979|6|Mentioned|p48, Fig. 44|Albian|Albian|SA unit that equates to part of the Coreena Member of Wallumbilla Formation in Qld.||||||07-FEB-11
26493|Coorikiana Sandstone|64048|6|Mentioned|p72|||South Australia equivalent to upper part of Wallumbilla Formation in Qld. Geological Province: Cooper Basin. Contains porous sandstones.||||||07-FEB-11
26493|Coorikiana Sandstone|64197|6|Mentioned|p625 Fig.1c, p630 Fig.6|Cretaceous|Cretaceous|Eromanga Basin. Mis-spelt as Cooriakana in Fig.1c.||Unit in Marree Subgroup.||Underlies Oodnadatta Formation; overlies Bulldog Shale.||10-DEC-15
26493|Coorikiana Sandstone|65385|5|Briefly described|pS134 Fig.7|Early Cretaceous|Early Cretaceous|Of Eromanga Basin. Overlies Bulldog Shale. Overlain by Oodnadatta Formation.||||||08-MAR-12
26493|Coorikiana Sandstone|65489|6|Mentioned|p96, p155|Early Cretaceous|Early Cretaceous|Eromanga Basin. 20m thick. Hosts gas discovery.  ||||Overlies Bulldog Shale. Is overlain by Oodnadatta Formation.||
26493|Coorikiana Sandstone|65925|5|Briefly described|Appendix 2.||||||||Fine-grained, calcareous, clayey sandstone; sandy siltstone; minor siltstone.|
26493|Coorikiana Sandstone|66518|5|Briefly described|p19.|Cretaceous|Cretaceous|Eromanga Basin.||Unit in Marree Subgroup.||Occurs locally between underlying Bulldog Shale and overlying Oodnadatta Formation.||
26493|Coorikiana Sandstone|66529|6|Mentioned|p12 Fig.5|||||Unit in Neales River Group.||||
26493|Coorikiana Sandstone|66623|6|Mentioned|p262.|||Equivalent to Coreena Member in NSW.||Unit in Rolling Downs Group in South Australia.||||
26493|Coorikiana Sandstone|67120|5|Briefly described|Map legend|Cretaceous|Cretaceous||||||Sandstone, fine-grained, calcareous, clayey; sandy siltstone; minor siltstone.|
26493|Coorikiana Sandstone|67462|5|Briefly described|Map legend.|Early Cretaceous|Early Cretaceous|Eromanga Basin.||||Overlies Bulldog Shale. Is overlain by Oodnadatta Formation.||
26493|Coorikiana Sandstone|67784|5|Briefly described|p26|Albian|Albian|Southern Eromanga Basin.||||Overlies Bulldog Shale. Is overlain by Oodnadatta Formation.||
26493|Coorikiana Sandstone|68068|5|Briefly described|Map legend|Albian|Albian|Eromanga Basin. Subsurface only. Shoreface to open marine.||Unit in Marree Subgroup.||Conformably and gradationally overlies Bulldog Shale. Is overlain conformably by Oodnadatta Formation.|Silty fine- to medium-grained sand, broadly cross-bedded, buff to yellow.|
26493|Coorikiana Sandstone|68713|6|Mentioned|p22|Cretaceous|Cretaceous|||Of the Marree Subgroup.||||
26493|Coorikiana Sandstone|68715|6|Mentioned|p31 Fig.7|Albian|Albian|||||||
26493|Coorikiana Sandstone|68734|5|Briefly described|p218 Fig.2, p221 Fig.3|Albian|Albian|Eromanga Basin (SW). Shallow marine.||Of the Rolling Downs Group.||||
26493|Coorikiana Sandstone|69019|3|Fully described|p85 Fig.21, p97-98.|Albian|Albian|SW Eromanga Basin. Originally defined as a Member of Oodnadatta Formation (Freytag, 1966); elevated to Formation status by Thomson (1980). Type area along Coorikiana Creek, ~40 km SW of Oodnadatta. Thickness varies from <1 to 36 m. Locally an important aquifer.||Unit in Marree Subgroup.||Overlies Bulldog Shale conformably. Is overlain conformably by Oodnadatta Formation.|Coarsening-upwards succession of greenish-white to grey, fine- to very fine-grained sandstone; glauconitic, bioturbated and broadly cross-bedded; sandy siltstone and minor siltstone interbeds; weathers buff to yellow.|
26493|Coorikiana Sandstone|69023|5|Briefly described|p89 Fig.20, p93, p99-100, p102-104, p151|Albian|Albian|See also p191-192. Originally part of Oodnadatta Formation (Freytag, 1966); elevated to Formation status by Thomson (1980). Thickness from <1 to c.35m. Stratigraphic wells intersection data.||Unit in Marree Subgroup.||Conformably overlies Bulldog Shale. Is overlain conformably by Oodnadatta Formation.|A coarsening-upwards succession of greenish-white to grey, glauconitic, bioturbated, cross-bedded fine- to very fine-grained sandstone and silty sandstone; minor siltstone interbeds.|
26493|Coorikiana Sandstone|69457|5|Briefly described|p41:3, 6-8|Early Cretaceous|Early Cretaceous|Thomson (1980); Moore and Pitt (1982). Eromanga Basin. Has not been recognised in the NT; the Wilgunya Subgroup nomenclature is thus preferred to the Marree Subgroup.||Marree Subgroup.||Overlies Bulldog Shale. Is overlain by Oodnadatta Formation.||12-JUL-16
26493|Coorikiana Sandstone|69673|6|Mentioned|p155 fig 127|Cretaceous|Cretaceous|||||Overlies Bulldog Shale, overlain by Oodnadatta Formation||
26493|Coorikiana Sandstone|69797|5|Briefly described|p17 Fig.2|Early Cretaceous|Early Cretaceous|Geol. Prov: Eromanga Basin.||||||
26493|Coorikiana Sandstone|69946|3|Fully described|p21-23, p57, p94, p113-119|Albian|Albian|Moore and Pitt (1982). Previously defined as a Member of Oodnadatta Formation by Freytag (1966), whose type section in Coorikiana Creek, 40km SW of Oodnadatta, still applies. Moore, Pitt et al. (1986) designated a subsurface reference section from 1123 to 1131m in Dullingari 1. Typically <20m thick. Wireline log correlations.||Unit in Marree Subgroup.||Conformably overlies Bulldog Shale. Is overlain conformably by Oodnadatta Formation. Passes laterally into Wallumbilla Formation and Marree Subgroup.|Fine-grained, silty, glauconitic, feldspathic and lithic sandstone; minor conglomerate with dark grey siltstone and mudstone interbeds at the base.|
26493|Coorikiana Sandstone|69947|5|Briefly described|p9, p13 Fig.7.2|Early Cretaceous|Early Cretaceous|Eromanga Basin. Shoreline deposits.||Marree Subgroup.||Overlies Bulldog Shale.||
26493|Coorikiana Sandstone|69948|6|Mentioned|Fig.4.1|||Eromanga Basin.||||||
26493|Coorikiana Sandstone|70336|5|Briefly described|Map legend|Cretaceous|Cretaceous|||Of Marree Subgroup.|||Fine-grained, calcareous, clayey sandstone; sandy siltstone; minor siltstone.|12-JAN-16
26493|Coorikiana Sandstone|70384|5|Briefly described|Map legend.|Cretaceous|Cretaceous|Eromanga Basin.||Marree Subgroup.||Gradationally overlies Bulldog Shale.|Mostly subsurface: silty fine- to medium-grained sand, broadly cross-bedded, buff to yellow.|
26493|Coorikiana Sandstone|70821|5|Briefly described|p21 Fig.2.6, p23|Early Cretaceous|Early Cretaceous|Eromanga Basin.||||Overlies Bulldog Shale. Is overlain by Oodnadatta Formation.||
26493|Coorikiana Sandstone|70823|5|Briefly described|p43-p44|Early Cretaceous|Early Cretaceous|Eromanga Basin. Up to 20m thick. Deposited in a regressive marine, shoreface environment.||||Overlies the Bulldog Shale. Overlain by the Oodnadatta Formation.||
26493|Coorikiana Sandstone|70860|6|Mentioned|p281|||Great Artesian Basin. Mis-spelled as Coorikianna Sandstone.||||||
26493|Coorikiana Sandstone|70938|5|Briefly described|p807-808|Early Cretaceous|Early Cretaceous|||Neales River Group.||||
26493|Coorikiana Sandstone|71321|6|Mentioned|p15, p65|||Of Eromanga Basin.||||||24-OCT-19
26493|Coorikiana Sandstone|71342|3|Fully described|Ch1 p19, Ch4 p8, Ch5 p21-p23|Albian|Albian|Originally defined as a member of the Oodnadatta Formation by Freytag (1966) before being elevated to formation status by Moore and Pitt (1982). A type section in Coorikiana Creek was given by Freytag (1966) and a reference section in Dullingari 11 by Moore, Pitt et al (1986). Outcrop, distribution and wireline log characteristics are discussed. Typically less than 20m thick. Sedimentology is discussed briefly. This unit is interpreted to have been deposited in a regressive marine, shoreface environment; however, it should be noted that Alley and White (1996) argue for a middle Albian marine transgressive setting instead. Spore-pollen zone is given in Ch5 p57 and elaborated on in Ch6 p9. Hosts commerically producible oil in Ulandi 12. See also Ch5 p33, Ch5 p57, Ch5 p114-p120, Ch6 p9-p10, Ch7 p10, Ch7 p13, Ch9 p4, Ch9 p9, Ch9 p11, Ch11 p2, Ch11 p5, Ch13 p2.||Marree Subgroup||Conformably overlies the Bulldog Shale. Conformably overlain by the Oodnadatta Formation. Laterally equivalent to the Wallumbilla Formation.|Fine-grained, silty, glauconitic, feldspathic and lithic sandstone with minor conglomerate and dark grey siltstone and mudstone interbeds at the base.|
26493|Coorikiana Sandstone|72298|5|Briefly described|p801|Cretaceous|Cretaceous|Eromanga Basin (SA).||Neales River Group.||Overlies Bulldog Shale. Is overlain by Oodnadatta FZ.||
26493|Coorikiana Sandstone|72456|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Marree 1:250k map sheet. |||||Sandstone, fine-grained, calcareous, clayey sandy siltstone; minor siltstone.|
26493|Coorikiana Sandstone|73167|6|Mentioned|p664 Fig. 2|Cretaceous|Cretaceous|Eromanga Basin. Contains gas.||||||
26493|Coorikiana Sandstone|73249|4|Described|p316-319, p320 Fig.2, p321-324, p326-338|Albian|Albian|Eromanga Basin. Early Albian age. Deposited during a partial marine regression to the southwest of the basin, subtidal to beach and fluvial environment. Typically 20m thick. Dominant clay mineral is montmorillonite, deposited in a more arid, warmer envionment than the Cadna-owie Formation. Unit described as sandstone dominated by other authors (Cotton et al., 2006; van der Weilen et al., 2011) but is mostly clay-rich in the samples studied. Sediment sources interpreted to be a mix of felsic to mafic igneous rocks. [Specific locations in text include p324 Fig.4, p334 Tb.7 and p337 Fig.9.]. See also misspelling Coorkiana Sandstone p322.||||Conformably overlies the Bulldog Shale, conformably underlies the Oodnadatta Formation, lateral equivalent of the Toolebuc Formation.|Sandstone with interbedded siltstone and mudstone, typically 20m thick.|
26493|Coorikiana Sandstone|73251|6|Mentioned|p36, p62|Early Cretaceous|Early Cretaceous|Eromanga Basin, Frome Embayment. Marginal thermal maturity. Contains[?] gas.||||Underlain by Bulldog Shale. Overlain by Oodnadatta Formation. Equivalent to Wallumbilla Formation.||
26493|Coorikiana Sandstone|73343|6|Mentioned|p337|Cretaceous|Cretaceous|Eromanga Basin. Hosts gas.||||Underlain by Bulldog Shale. Overlain by Oodnadatta Formation. Equivalent to Wallumbilla Formation.||
26493|Coorikiana Sandstone|73479|5|Briefly described|p156 Fig.2, p159, p175|Cretaceous|Cretaceous|Eromanga Basin. Shoreface depositional environment.|ca 105 Ma|||Overlies Bulldog Shale, underlies Oodnadatta Formation||
28474|Cooyerdoo Granite|40448|6|Mentioned|p34|||Of Moody Suite.||||||21-JAN-10
28474|Cooyerdoo Granite|65915|4|Described|p4 Fig.3, p6-12, p16-19|Mesoarchean|Mesoarchean|High-K, I-type granite. Scattered outcrops over ~20x7 km. Outcrops as pavements and low tors. Even-grained, medium-grained, grey, quartz- and K-feldspar-dominated granite with subsidiary plagioclase and biotite. Adjacent to Middleback Subgroup and Myola Volcanics. SHRIMP U-Pb zircon age of 3157+/-2 Ma. Geochemical analyses detailed.||||||
28474|Cooyerdoo Granite|66302|6|Mentioned|p14, p34, p60, p84, p85|Mesoarchean|Mesoarchean|Obsolete name. [the unit which supersedes it is not named in this article]. Intrudes unkown older crust. Contains inherited zircons aged at ca. 3300 Ma. |`3150 Ma|||||
28474|Cooyerdoo Granite|66882|5|Briefly described|p100, p102 Fig.2, p116|Mesoarchean|Mesoarchean|Middleback Range. Forms basement to metasedimentary rocks. Possible source of sediments (and zircons) for Cook Gap Schist.|c.3150 Ma|||||
28474|Cooyerdoo Granite|67721|5|Briefly described|p33 Fig.2, p36|Mesoarchean|Mesoarchean||c. 3150 Ma (Fraser et al. 2010)|||||
28474|Cooyerdoo Granite|68158|5|Briefly described|p2|||Middleback Range, Gawler Craton. Basement to the Middleback Subgroup.|3150 Ma (Fraser et al., 2010).|||||
28474|Cooyerdoo Granite|68208|3|Fully described|p31-40|Mesoarchean|Mesoarchean|Name first published by Parker, Fanning & Flint 1985. This article is intended to define the unit now recognised as the oldest granite in South Australia. A type area is nominated, but boundary relationships are not exposed, and full extent is uncertain at present.|3157 +/- 2 Ma, 3149 +/-3 Ma U-Pb zircon|||Presumably intruded by foliated dolerite dykes between crystallisation and deformation of granite (~3150 and 2500 Ma), oriented sub-parallel to foliation in Cooyerdoo Granite. No contacts observed.|Medium-grained, foliated, calc-alkaline, I-type granite, with deformation increasing from east to west, from foliated granite to gneissic granite.|23-JUL-13
28474|Cooyerdoo Granite|69048|6|Mentioned|p3|Archean|Archean|Eyre Peninsula / Yorke Peninsula.||||||
28474|Cooyerdoo Granite|70027|6|Mentioned|p56,71|Archean|Archean|Geological province: Gawler Craton. Possible source of 3200-3100 Ma detrital zircons in the Gawler Craton.|Mesoarchean|Mesoarchean||||17-JUL-19
28474|Cooyerdoo Granite|70286|6|Mentioned|p884|Mesoarchean|Mesoarchean|Eastern Gawler Craton.|c.3150 Ma.|||||
28474|Cooyerdoo Granite|70334|5|Briefly described|p74|Mesoarchean|Mesoarchean|Geological province: Gawler Craton. Basement to the Gawler Craton.|c. 3150 Ma|||Equivalent to Sleaford Complex.||
28474|Cooyerdoo Granite|70382|6|Mentioned|p32|Archean|Archean|yre Peninsula region. Possible source for some of Quartoo Sand Member inherited zircon.|~3250-3150 Ma |||||
28474|Cooyerdoo Granite|70659|6|Mentioned|p10|Archean|Archean|||||||
28474|Cooyerdoo Granite|70721|5|Briefly described|p63-p64|Mesoarchean|Mesoarchean|Spencer Domain, Gawler Craton. Basement of the Spencer Domain.|c. 3150 Ma|||Faulted against Myola Volcanics and Broadview Schist.||
28474|Cooyerdoo Granite|70816|5|Briefly described|p3-4|Mesoarchean|Mesoarchean|Geological province: Gawler Ranges. Basement to the Spencer Domain.|~3150 Ma (McAvaney 2012; Fraser et al, 2010)|||Overlain by Hutchison Group. In faulted contact to the east with Myola Volcanics, Broadview Schist and Tip Top Granite.||30-MAY-19
28474|Cooyerdoo Granite|70948|5|Briefly described|p974-975|Mesoarchean|Mesoarchean|Geological province: Gawler Craton. Basement to the Spencer Domain.|ca. 3150 Ma|||Overlain by iron formations of the Hutchison Group. In faulted contact with the Myola Volcanics (ca 1790 Ma), Broadview Schist, and Tip Top Granite (ca 1775 Ma).||
28474|Cooyerdoo Granite|71037|6|Mentioned|p21 Fig.1|Archean|Archean|Shown only on 'Outcropping geology and mineral deposits of northern Eyre Peninsula' map p21 Fig.1. These Archean rocks are shown in the southeastern part of the Eyre Peninsular.||||Shown as older than Coolanie Gneiss.|Granite.|
28474|Cooyerdoo Granite|71129|5|Briefly described|p14,17-19,23,41,203-205|Mesoarchean|Mesoarchean|Geological Province: Spencer Domain, Gawler Craton. Basement to the Broadview Schist.|c. 3150 Ma (Spencer et al., 2010b)|||Overlain by Broadview Schist and the Sleaford Complex.||13-NOV-19
28474|Cooyerdoo Granite|71317|5|Briefly described|p14, p16|Mesoarchean|Mesoarchean|Spencer Domain, Gawler Craton.|c. 3150 Ma (Fraser et al., 2010)|||||
28474|Cooyerdoo Granite|71322|6|Mentioned|p91|Mesoarchean|Mesoarchean||c.3150 Ma.|||||
28474|Cooyerdoo Granite|71349|6|Mentioned|p738|Archean|Archean|Gawler Craton.|c.3.1 Ga.|||||
28474|Cooyerdoo Granite|71413|6|Mentioned|p32 Fig 2|||Geological province: Gawler Craton. ||||||
28474|Cooyerdoo Granite|71534|5|Briefly described|p295-296,301,303|Mesoarchean|Mesoarchean|Geological province: Gawler Craton. Associated with more evolved magmatism; sits adjacent to Donington Suite and broadly corresponds in location to the Kalinjala Shear Zone.|c. 3150 Ma|||||
28474|Cooyerdoo Granite|71536|5|Briefly described|p1, p89, p92|||Occurs on the Whyalla 250k and Cowell 100k map sheets.|||||Quartzofeldspathic gneiss.|
28474|Cooyerdoo Granite|71559|6|Mentioned|p15 Fig 1|Archean|Archean|Geological province: Gawler Craton.||||||
28474|Cooyerdoo Granite|71859|4|Described|p1-p4, p6, p18, p24, p28|Mesoarchean|Mesoarchean|Southern Gawler Craton, Spencer Domain. Forms basement in the Gawler Craton and is the oldest exposed unit in the entire craton (only outcrops on northern Eyre Peninsula). Interpreted to have been derived from melting of tonalite-trondhjemite-granodiorite crust.|c. 3150 Ma|||Overlain by the Sleaford and Mulgathing complexes.||
28474|Cooyerdoo Granite|71862|5|Briefly described|p1-p4, p7-p8, p10, p21, p44, p54, p58|Mesoarchean|Mesoarchean|Originally a part of the now obsolete Lincoln Complex. This unit is the oldest exposed basement of the Gawler Craton and outcrops on the northeastern Eyre Peninsula. Geochemical relationship with the Moola and Pinbong suites are discussed.|c. 3150 Ma|||Intruded by (interpreted) the Burkitt Granite.||18-APR-23
28474|Cooyerdoo Granite|72058|4|Described|p170-p173, p174, p176,p177, p179|Archean|Archean|Northern Middleback Ranges, Gawler Craton. This unit is the oldest basement rock discovered in the Gawler Craton. Outcrops in an area of high magnetic intensity known as the Spencer Domain. Whole rock geochemistry is provided. Zircon morphology and analysis is described. U-Pb SHRIMP crystallisation age determined from sample MB63-64 as 3134+/-18 Ma from the two oldest grains analysed. See also p181, p184-p186, p190, p192.|3134+/-18 Ma (min. cryst)||||I-type, medium grained granites consisting of alkali feldspars and quartz that is variably altered.|16-MAR-21
28474|Cooyerdoo Granite|72090|6|Mentioned|p11|Mesoarchean|Mesoarchean|Olympic Domain, Gawler Craton.|c. 3150 Ma|||||
28474|Cooyerdoo Granite|72462|6|Mentioned|p3|Archean|Archean|Gawler Craton.||||||
28474|Cooyerdoo Granite|72463|6|Mentioned|p2|Archean|Archean|||||||
28474|Cooyerdoo Granite|72484|5|Briefly described|p2-3, 19-21, 23|||Basement to Middleback Ranges area of Gawler Craton.|~3100 Ma (Fraser et al., 2010).|||Is overlain by Hutchison Group.||
28474|Cooyerdoo Granite|73026|5|Briefly described|p3, p4 fig 1.2, p5-6|Mesoarchean|Mesoarchean|Occurs on the northeastern Eyre peninsula. Characteristically elevated LILE and LREE contents and low Na/K. May be post-tectonic in origin and a product of melting of pre-existing tonalite-trondhjemite-granodiorite crust.|c. 3250-3150 Ma||||granite, gneisses, felsic and minor mafic.|
28474|Cooyerdoo Granite|73027|5|Briefly described|p4, p6, p9|Mesoarchaean|Mesoarchaean|Eastern Eyre Peninsula/Yorke Peninsula.|c. 3250-3150 Ma||||Granite and associated gneisses, felsic and minor mafics.|
28474|Cooyerdoo Granite|73030|6|Mentioned|p2149|Mesoarchean|Mesoarchean|Gawler Craton.||||||
28474|Cooyerdoo Granite|73103|5|Briefly described|Map legend.|Archean|Archean||3157 +/- 2 Ma (U-Pb).||||Granite, medium-grained, K-feldspar + plagioclase + quartz + biotite + minor opaques; weakly lineated and foliated; feldspar and quartz-rich leucocratic bands; biotite-rich schlieren; granodioritic compositional banding.|
28474|Cooyerdoo Granite|73110|5|Briefly described|Map legend.|Archean|Archean||3157 +/- 2 Ma (U-Pb).||||Granite, medium-grained, K-feldspar + plagioclase + quartz + biotite + minor opaques; weakly lineated and foliated feldspar and quartz-rich leucocratic bands; biotite-rich schlieren; granodioritic compositional banding.|
28474|Cooyerdoo Granite|73130|6|Mentioned|[poster] Fig.1|Archean|Archean|||||||28-OCT-22
28474|Cooyerdoo Granite|73162|6|Mentioned|p449, Fig.1|Mesoarchean|Mesoarchean||3150 Ma|||||
28474|Cooyerdoo Granite|73165|6|Mentioned|p621, p634 Fig. 11|Mesoarchean|Mesoarchean|Gawler Craton. Oldest known units within the Gawler Craton. Cooyerdroo Granite in Fig. 11, p634.|ca 3200 - 3150 Ma||||Granitoids.|
28474|Cooyerdoo Granite|73234|6|Mentioned|p18|||Part of the oldest known basement of the Gawler Craton.||||||
28474|Cooyerdoo Granite|73235|6|Mentioned|p53|Mesoarchean|Mesoarchean|Gawler Craton. Spencer region.|3150 Ma|||||
28474|Cooyerdoo Granite|73302|6|Mentioned|p32-33|||Part of the basement to the Gawler Craton.|c.3150 Ma.|||||
28474|Cooyerdoo Granite|73493|5|Briefly described|p716 Fig.3|||Gawler Craton.|||||Granitic.|
38349|Corny Point Paragneiss|23803|2|Defined|p32|Paleoproterozoic|Paleoproterozoic|Layered migmatite. Intruded by the Donington Granitoid Suite. Age: ~2000-1845Ma. Not equivalent to the unpublished "Corny Point augen gneiss" of Webb (1978). Geological Province: Gawler Craton.||||||04-AUG-09
38349|Corny Point Paragneiss|24585|5|Briefly described|p32|Paleoproterozoic|Paleoproterozoic|Layered migmatite. Contains a Hutchison Group equivalent protolith (1920-1860Ma).||||||07-NOV-08
38349|Corny Point Paragneiss|60958|5|Briefly described|Map Legned|Paleoproterozoic|Paleoproterozoic|Migmatitic layered paragneiss, dark grey to white-grey, with coarse grained quartz, plagioclase, biotite, alkali feldspar. Metamorphic age: 1845 +/- 6Ma. Deposition ~1920-1860Ma. Geological Province: Gawler Craton.||||||07-NOV-08
38349|Corny Point Paragneiss|61121|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Migmatitic layered paragneiss, dark grey to white-grey, with coarse-grained quartz, plagioclase, biotite, alkali feldspar, garnet, sillimanite, +/-orthoclase, +/-clinopyroxene, +/-cordierite, +/-spinel, +/-corundum. Age: ~1920-1860Ma. Geol.Prov: Gawler C||||||04-AUG-09
38349|Corny Point Paragneiss|63223|5|Briefly described|p16, p18, p19|Paleoproterozoic||Max. depositional age: interpreted to be 1889+/-11Ma. Intruded by the Donington Suite Metasedimentary rock: coarse-grained garnet porphyroblasts with biotite-quartz-cordierite-felspar gneiss at Corny Point. Geological Province: Gawler Craton.||||||04-AUG-09
38349|Corny Point Paragneiss|63398|5|Briefly described|p663|Paleoproterozoic|Paleoproterozoic|Migmatitic paragneisses. Probable equivalent of Hutchison Group and of the gneissic and granitoid rocks of Donington Suite. ||||||07-NOV-08
38349|Corny Point Paragneiss|64233|5|Briefly described|p25|Paleoproterozoic|Paleoproterozoic|Age: 1889-1850+/-11Ma. On SW tip of Yorke Peninsula.||||||07-NOV-08
38349|Corny Point Paragneiss|64282|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Geol Prov: Gawler Craton/Yorke Peninsula. Deposition age: 1860-1820Ma. Metamorphic age: 1845+/-6Ma.Migmatite layered paragneiss, dark grey to white-grey, with coarse-grained quartz, plagioclase, biotite, alkali feldspar, garnet, sillimanite.....etc.||||||02-MAR-15
38349|Corny Point Paragneiss|64313|5|Briefly described|p452, p457 Fig. 6|Paleoproterozoic|Paleoproterozoic|Metasedimentary rocks at Corny Point, on Yorke Peninsula. Ages: 1824+/-18Ma and 1827+/-18Ma. See also p461, p463-465.||||||09-FEB-10
38349|Corny Point Paragneiss|65219|6|Mentioned|p29, p30 Fig.4|Paleoproterzoic|Paleoproterzoic|Detrital zircon ages as young as 1870 Ma.||||||22-SEP-09
38349|Corny Point Paragneiss|65375|4|Described|p7, pp12-14,  pp44-45.|Paleoproterozoic|Paleoproterozoic|Oldest rocks on Yorke Peninsula. Has a Hutchison Group equivalent protolith; metamorphosed c.1845 Ma.  Fine-grained meta-argillite and calc-silicate lenses as boudins up to 2m across.|c.1920-1845 +/- 6 Ma.|||Intruded by foliated amphibolite and Gleesons Landing Granite.|Migmatitic paragneiss consisting of dark-grey to white-grey, coarse-grained, layered migmatites of quartz, plagioclase, biotite, alkali feldspar, garnet, sillimanite(-orthopyroxene-clinopyroxene-cordierite-spinel-corundum).|
38349|Corny Point Paragneiss|65390|6|Mentioned|p20, p23 Fig.3|Orosirian|Orosirian|Metamorphic zircons formed in this unit at c.1850 Ma during the Neill Event.||||||
38349|Corny Point Paragneiss|66302|5|Briefly described|p27, p33|Orosirian|Orosirian|Spencer Domain, Gawler Craton. Protoliths believed to have been deposited between 1870-1850 Ma (Howard et al, 2009). Detrital zircon peaks occur at 2510, 2450 and 2000 Ma.  Metamorphosed and deformed during the Cornian Orogeny. |||||Layered migmatite|
38349|Corny Point Paragneiss|66882|5|Briefly described|p102 Fig.2, p114 Fig.11, p116-117, p119|Orosirian|Orosirian|SW Yorke Peninsula. Possible source rocks for c.2000 Ma zircons in Cleve Group.|1870-1850 Ma|||||
38349|Corny Point Paragneiss|67536|6|Mentioned|Map Legend|||Gawler Craton. Precursor possibly Hutchison Group equivalent.|||||Migmatitic paragneiss.|
38349|Corny Point Paragneiss|68131|5|Briefly described|p3 Tb.1, p6, p12, p31-37|||SW Yorke Peninsula. This age is interpreted to be the crystallisation age of the leucosome, supporting the conclusion of Zang and Fanning (2001) that the Donington Suite underwent upper amphibolite metamorphism at c.1850 Ma.|1848 +/- 8 Ma (SHRIMP, magmatic age)|Donington Suite.|||Contains prominent garnet-bearing leucosome networks.|13-MAY-20
38349|Corny Point Paragneiss|69048|6|Mentioned|p3|||Eyre Peninsula / Yorke Peninsula.|c.1875 Ma.|||||
38349|Corny Point Paragneiss|70027|6|Mentioned|p56|Paleoproterozoic|Paleoproterozoic|Geological province: Gawler Craton.||||||
38349|Corny Point Paragneiss|71129|5|Briefly described|p14,18,p35, 203|Orosirian|Orosirian|Geological Province: Olympic Domain, Gawler Craton. Basement to Moonabie and Wandearah formations.|c. 1890 Ma|||Overlain by Wallaroo Group.||13-NOV-19
38349|Corny Point Paragneiss|71317|5|Briefly described|p16||Palaeoproterozoic|Olympic Domain, Gawler Craton.|<1890 Ma|||||
38349|Corny Point Paragneiss|71348|6|Mentioned|p201|Orosirian|Orosirian|Geological province: Gawler Craton.||||||
38349|Corny Point Paragneiss|71534|6|Mentioned|p296|Orosirian|Orosirian|Geological province: Gawler Craton.||||||
38349|Corny Point Paragneiss|71536|6|Mentioned|p1, p99, p102-p103|||||||||
38349|Corny Point Paragneiss|71859|5|Briefly described|p4, p6||Orosirian|Olympic Domain, southern Gawler Craton.|<1900 Ma|||||
38349|Corny Point Paragneiss|72090|6|Mentioned|p10|Orosirian|Orosirian|Olympic Domain, Gawler Craton.|<1890 Ma|||||
38349|Corny Point Paragneiss|73026|5|Briefly described|p6, p9-10|Paleoproterozoic|Paleoproterozoic|Eyre Peninsula/Yorke Peninsula.|c. 1875 Ma||||Paragneiss, migmatitic.|
38349|Corny Point Paragneiss|73027|5|Briefly described|p6, p9|Palaeoproterozoic|Palaeoproterozoic||c. 1870 Ma||||Paragneiss, migmatitic.|
38349|Corny Point Paragneiss|73030|6|Mentioned|p2149|Orosirian|Orosirian|Gawler Craton, Olympic Cu-Au Province.||||||
38349|Corny Point Paragneiss|73092|6|Mentioned|p2, p35|Paleoproterozoic|Paleoproterozoic|May include a c. 2100 Ma detrital zircon population.||||||
38349|Corny Point Paragneiss|73107|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Gawler Craton: Yorke Peninsula, islands of Investigator Strait and DDH Investigator 1. Metamorphic age 1845 +/- 6 Ma.|~1920-1860 Ma (deposition age).|Donington Suite.||Protolith possibly equivalent to Hutchison Group. Is intruded by (the granodiorite facies of) Gleesons Landing Granite.|Migmatitic layered paragneiss, dark grey to white-grey, with coarse-grained quartz, plagioclase, biotite, alkali feldspar, garnet, sillimanite, +/- orthopyroxene, +/- cordierite, +/- spinel, +/- corundum.|
38349|Corny Point Paragneiss|73122|5|Briefly described|p20, 23, 28, 41|||Southern Yorke Peninsula. Its age is also given as 2000-1845 Ma. Appears on p41 as the Corning Point Paragneisses.|~1870 Ma.||||A layered migmatite. Deformed by Cornian and Kimban Orogenies.|
38349|Corny Point Paragneiss|73130|6|Mentioned|[poster] Fig.1|Paleoproterozoic|Paleoproterozoic|||||||28-OCT-22
38349|Corny Point Paragneiss|73165|6|Mentioned|p635||||||||Migmatitic gneisses.|
38349|Corny Point Paragneiss|73235|6|Mentioned|p53|Orosirian|Orosirian|Gawler Craton. Olympic region.|1920-1860 Ma|||||
38349|Corny Point Paragneiss|73493|5|Briefly described|p716 Fig.3|||Gawler Craton.|||||Sandstone, shale, siltone or schist.|
38349|Corny Point Paragneiss|73525|5|Briefly described|p19 Fig.13|Orosirian|Orosirian|Olympic Domain.|1889+/-4 Ma MDA, 1845+/-6 metamorphic age||||Metamorphics.|
38349|Corny Point Paragneiss|73644|6|Mentioned|p2-3|Paleoproterozoic|Paleoproterozoic|Protolith deposited c. 1890-1850 Ma, metamorphosed during the c. 1850 Ma Cornian Orogeny.|c. 1890-1850 Ma||||Upper amphibolite/granulite facies.|
27380|Corraberra Sandstone Member|23287|6|Mentioned|Fig.2|||Age: Lower Ediacarian. of Stuart Shelf.||||||
27380|Corraberra Sandstone Member|23805|5|Briefly described|p5 Fig. 3|Neoproterozoic|Neoproterozoic|Of the Tent Hill Formation (Wilpena Group).  Geological Province: Gawler Craton.||||||
27380|Corraberra Sandstone Member|24195|5|Briefly described|p42, 44|||Considered as lateral equivalent of Bayley Range Siltstone Member. Parent: Tent Hill Formation. Geological Province: Adelaide Geosyncline||||||
27380|Corraberra Sandstone Member|24321|5|Briefly described|Map legend|Late Adelaidean|Late Adelaidean|Parent: Tent Hill Formation||||||
27380|Corraberra Sandstone Member|30801|6|Mentioned|p5|||Tent Hill Formation. Table P5-6||||||
27380|Corraberra Sandstone Member|30807|6|Mentioned|p102|||Suggested map symbol||||||
27380|Corraberra Sandstone Member|31395|6|Mentioned|p64|||||||||
27380|Corraberra Sandstone Member|31419|6|Mentioned|p33|||||||||
27380|Corraberra Sandstone Member|31540|4|Described|p10|||||||||
27380|Corraberra Sandstone Member|32507|6|Mentioned|Table 3|||||||||
27380|Corraberra Sandstone Member|33474|6|Mentioned|Fig.3|||||||||
27380|Corraberra Sandstone Member|34536|6|Mentioned|Map legend|Adelaidean|Adelaidean|Marinoan||||||
27380|Corraberra Sandstone Member|35130|6|Mentioned|p7|||||||||
27380|Corraberra Sandstone Member|37461|6|Mentioned|Table 5.I|||||||||
27380|Corraberra Sandstone Member|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Marinoan||||||
27380|Corraberra Sandstone Member|39808|6|Mentioned|p223|||||||||
27380|Corraberra Sandstone Member|40448|5|Briefly described|p38|||||||||
27380|Corraberra Sandstone Member|41429|4|Described|p224|||||||||
27380|Corraberra Sandstone Member|41507|6|Mentioned|p17|||||||||
27380|Corraberra Sandstone Member|41526|6|Mentioned|p56|||||||||
27380|Corraberra Sandstone Member|42222|6|Mentioned|Table 1 P4|||||||||
27380|Corraberra Sandstone Member|42465|5|Briefly described|Map legend|Adelaidean (Marinoan)||||||||
27380|Corraberra Sandstone Member|42469|4|Described|p24|||||||||
27380|Corraberra Sandstone Member|42600|6|Mentioned|p9|||of Tent Hill Formation||||||
27380|Corraberra Sandstone Member|42721|5|Briefly described|map legend|Marinoan||||||||
27380|Corraberra Sandstone Member|43052|5|Briefly described|p192,table 6.1|||of Tent Hill Formation||||||
27380|Corraberra Sandstone Member|43094|4|Described|Table 5|||of Tent Hill Formation||||||
27380|Corraberra Sandstone Member|44660|14|Not recorded|map legend|||Marinoan, lithology.||||||
27380|Corraberra Sandstone Member|44934|5|Briefly described|Map Legend||Adelaidean|||||||
27380|Corraberra Sandstone Member|60955|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Of the Tent Hill Formation. Red-brown silty sandstones and flaggy, micaceous siltstones.||||||
27380|Corraberra Sandstone Member|67127|6|Mentioned|p104|Neoproterozoic|Neoproterozoic|South Australia.||Wilpena Group||Underlies the Arcoona Quartzite Member. Unconformably overlies the Roxby Downs Granite.||
27380|Corraberra Sandstone Member|67870|5|Briefly described|p18|||Mapped in the PORT AUGUSTA 1:250 000 geological map.||Tent Hill Formation.||Equivalent to ABC Quartzite and Brachina Formation.||
27380|Corraberra Sandstone Member|68131|6|Mentioned|p89|Neoproterozoic|Neoproterozoic|||||||
27380|Corraberra Sandstone Member|70333|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Parent Formation not named.|||||Sandstone, red, purple, slumped, silty. Some shale.|
27380|Corraberra Sandstone Member|70334|4|Described|p33,57-59,66,77,92|Ediacaran|Ediacaran|Geological province: Gawler Craton. Of Stuart Shelf. Deposited as deltaic sands prograding from the western edge of the Stuart Shelf. Intruded by unnamed Jurassic kimberlites.||Unit of Tent Hill Formation.||Underlain by Tregolana Shale Member.|Thin beds of red sandstone interbedded with red shales and siltstone, upper section of greyish-red, iron-stained, fine- to medium-grained sandstone interbedded with greyish-brown shale.|14-OCT-19
27380|Corraberra Sandstone Member|70406|4|Described|p123-124, 119-121, 126, 127, 128, 117|Neoproterozoic|Neoproterozoic|Redefined herein to exclude rocks now part of the Lincoln Gap Siltstone Member. ~25m thick. Shoreface sandstones. Deposited above fairweather wave base in a storm-dominated environment. See p126 - "The Corraberra Sandstone Member of Tent Hill Formation has an equivalent that is included in the Brachina Formation at Hallett Cove (Dyson 1995)". p117 also states a correlate relationship. Although, this relationship is shown in Figure 5 p121 (Dyson 1995) as to be part of both Tent Hill Formation and Brachina Formation.||Of Tent Hill Formation. Said to be also of Brachina Formation p121 and p126.||Disconformable over Lincoln Gap Siltstone Member. Grades upwards into Simmens Quartzite. Partial lateral equivalent to lower ABC Range Quartzite, upper Brachina Formation (Bayley Range Siltstone).|Greyish red iron-stained, fine to medium-grained sandstone interbedded with greyish brown shale. Sandstone commonly micaceous, show heavy mineral lamination, swaley cross-stratification, cross bedding.|12-MAY-16
27380|Corraberra Sandstone Member|71037|5|Briefly described|p22-23 Fig.2|Neoproterozoic|Neoproterozoic|Shown only on the Six Mile Hill 1:75,000 surface geology map (p22-23 Fig.2).||Tent Hill Formation||Overlies Lincoln Gap Siltstone Member and underlies Simmens Quartzite Member.|Yellowish brown, fine- to medium-grained laminated to cross-bedded sandstone; slumping.|
27380|Corraberra Sandstone Member|71129|4|Described|p128-129,131,133-134,138,164,209,225|Ediacaran|Ediacaran|Of Stuart Shelf. Deposition at or above fairweather wave base in a shoreface environment. Thickness: about 25m. [Indexed mistakenly as the Corroberra Sandstone Member].||Unit of Tent Hill Formation.||Gradationally overlain by Simmens Quartzite Member. Underlain disconformably by Lincoln Gap Siltstone Member. Correlable to Bayley Range Siltstone Member/Brachina Fm.|Greyish-red to chocolate-brown iron-stained fine- to medium-grained micaceous sandstone with interbedded greyish-brown shales; quasi-planar lamination, swaley cross-stratification and medium-scale cross-bedding is common, and heavy mineral laminae.|13-NOV-19
27380|Corraberra Sandstone Member|71131|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Age shown as Marinoan.||Tent Hill Formation.|||Yellowish-brown, fine- to medium-grained laminated to cross-bedded sandstone; slumping.|
27380|Corraberra Sandstone Member|71895|5|Briefly described|APP4. p4,|||See Corraberra Sandstone.||Wilpena Group||||
27380|Corraberra Sandstone Member|72247|5|Briefly described|p43|Neoproterozoic|Neoproterozoic|Of Adelaide Geosyncline.||Unit of Wilpena Group.||Overlain by Arcoona Quartzite or Simmens Quartzite Member. Underlain by Woomera Shale or Tregolana Shale Member.||
27380|Corraberra Sandstone Member|73110|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic||||||Sandstone, red, purple, slumped, silty. Some shale.|
27380|Corraberra Sandstone Member|73227|5|Briefly described|p25|||Torrens Hinge Zone and[?] Woomera area.||Tent Hill Formation, Wilpena Group||Underlain by 'Woomera Shale' and Tregolana Shale Member. Overlain by 'Arcoona Quartzite' and Simmens Quartzite Member.|Thin beds of purple-brown sandstone, siltstone and shale.|
27380|Corraberra Sandstone Member|73234|6|Mentioned|p6|||||Tent Hill Formation, Wilpena Group||||
27751|Corunna Conglomerate|22629|4|Described|fig2, p,152,158,162|Statherian|Statherian|||||||
27751|Corunna Conglomerate|22690|6|Mentioned|P305|||||||||
27751|Corunna Conglomerate|23481|5|Briefly described|p19 Fig 1|||Geological Province: Gawler Craton.||||||
27751|Corunna Conglomerate|23719|4|Described|p22|Mesoproterozoic|Mesoproterozoic|See also page 22 table 6. Overlain by Blue Range Beds. Underlain by Moonabie Formation. Geological Province: Gawler Craton.||||||28-FEB-08
27751|Corunna Conglomerate|23805|5|Briefly described|p4 Fig. 1|Mesoproterozoic|Mesoproterozoic|Geological Province: Gawler Craton.||||||
27751|Corunna Conglomerate|23818|6|Mentioned|p31|||Geological Province: Gawler Block.||||||
27751|Corunna Conglomerate|24197|6|Mentioned|p72|||Geological Province: Gawler Craton.||||||07-FEB-11
27751|Corunna Conglomerate|24261|5|Briefly described|p1047 Fig.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Gawler Craton||||||
27751|Corunna Conglomerate|24422|6|Mentioned|p84 Fig. 1|||Geological Province: Gawler Craton.||||||
27751|Corunna Conglomerate|24505|5|Briefly described|p5 Fig. 1|||Geological Province: Gawler Craton.||||||
27751|Corunna Conglomerate|24583|6|Mentioned|p12|||Considered Blue Range Beds equivalents.||||||
27751|Corunna Conglomerate|24597|5|Briefly described|p526 Fig. 1|Mesoproterozoic|Mesoproterozoic|Geological Province: Gawler Craton.||||||
27751|Corunna Conglomerate|30237|6|Mentioned|Fig.1|||||||||
27751|Corunna Conglomerate|30806|5|Briefly described|Table 1|||||||||
27751|Corunna Conglomerate|30807|6|Mentioned|p103|||Suggested map symbol||||||
27751|Corunna Conglomerate|30845|6|Mentioned|Fig.1|||||||||
27751|Corunna Conglomerate|31034|6|Mentioned|Fig. 2|||||||||
27751|Corunna Conglomerate|31248|6|Mentioned|p57|||Correlation||||||
27751|Corunna Conglomerate|31320|6|Mentioned|p13|||Carpentarian||||||
27751|Corunna Conglomerate|31542|6|Mentioned|p468|||||||||
27751|Corunna Conglomerate|32507|6|Mentioned|Table 3|||||||||
27751|Corunna Conglomerate|32561|6|Mentioned|Fig.4|||||||||
27751|Corunna Conglomerate|33468|6|Mentioned|Fig.3|||See also pp203, 205.||||||02-JUN-09
27751|Corunna Conglomerate|33470|5|Briefly described|p463|||||||||
27751|Corunna Conglomerate|33479|6|Mentioned|Fig.1|||||||||
27751|Corunna Conglomerate|33557|6|Mentioned|p12|||Overlies granites of Charlestonian phase.||||||02-JUN-09
27751|Corunna Conglomerate|34269|6|Mentioned|Table 1|||Lower Proterozoic.||||||
27751|Corunna Conglomerate|34287|6|Mentioned|p37|||||||||
27751|Corunna Conglomerate|34319|6|Mentioned|p69|||||||||
27751|Corunna Conglomerate|34535|6|Mentioned|Fig.16|||Carpentarian||||||
27751|Corunna Conglomerate|34537|5|Briefly described|p31|||Carp.||||||
27751|Corunna Conglomerate|34812|6|Mentioned|Table 9|||||||||
27751|Corunna Conglomerate|35078|6|Mentioned|p262|||||||||
27751|Corunna Conglomerate|35255|6|Mentioned|p7|||||||||
27751|Corunna Conglomerate|35270|6|Mentioned|Fig.1|||||||||
27751|Corunna Conglomerate|35298|5|Briefly described|Table 1|||||||||
27751|Corunna Conglomerate|35672|6|Mentioned|p9|||||||||
27751|Corunna Conglomerate|35706|6|Mentioned|Fig.1|||||||||
27751|Corunna Conglomerate|35772|6|Mentioned|p9|||||||||
27751|Corunna Conglomerate|36073|6|Mentioned|Fig.3|||||||||
27751|Corunna Conglomerate|36507|6|Mentioned|Fig.1|||||||||
27751|Corunna Conglomerate|36627|6|Mentioned|p82|||||||||
27751|Corunna Conglomerate|37461|6|Mentioned|p317|||||||||
27751|Corunna Conglomerate|37621|6|Mentioned|p12|||||||||
27751|Corunna Conglomerate|37811|6|Mentioned|p222|||||||||
27751|Corunna Conglomerate|38068|5|Briefly described|p67|||||||||
27751|Corunna Conglomerate|39344|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
27751|Corunna Conglomerate|39345|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
27751|Corunna Conglomerate|39349|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
27751|Corunna Conglomerate|39352|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
27751|Corunna Conglomerate|39802|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
27751|Corunna Conglomerate|40430|6|Mentioned|Fig.1|||||||||
27751|Corunna Conglomerate|40445|6|Mentioned|p53|||||||||
27751|Corunna Conglomerate|40448|5|Briefly described|p36|||||||||
27751|Corunna Conglomerate|40644|6|Mentioned|p120 Fig. 2, p121|Mesoproterozoic|Mesoproterozoic|Age: 1473+/-20Ma (on shale) - see table 4, p135.  Intracontinental, shallow water sequence; shale. See also p124 Fig. 3,  p135.||||||13-AUG-08
27751|Corunna Conglomerate|41125|6|Mentioned|p30|||||||||
27751|Corunna Conglomerate|41402|6|Mentioned|p35|||||||||
27751|Corunna Conglomerate|41493|6|Mentioned|Table 1|||||||||
27751|Corunna Conglomerate|41609|6|Mentioned|Fig.1|||||||||
27751|Corunna Conglomerate|41619|6|Mentioned|Map legend|Mesoproterozoic||||||||
27751|Corunna Conglomerate|41667|4|Described|p73|||||||||
27751|Corunna Conglomerate|41972|6|Mentioned|p377|||||||||
27751|Corunna Conglomerate|41995|6|Mentioned|p17|||||||||
27751|Corunna Conglomerate|42167|6|Mentioned|Fig.4 P117|||||||||
27751|Corunna Conglomerate|42239|6|Mentioned|p152|||||||||
27751|Corunna Conglomerate|42283|6|Mentioned|Fig.5 P82|||||||||
27751|Corunna Conglomerate|42357|6|Mentioned|p8|||||||||
27751|Corunna Conglomerate|42546|5|Briefly described|Map legend|Mesoproterozoic||||||||
27751|Corunna Conglomerate|42736|5|Briefly described|map legend|Mesoproterozoic||||||||
27751|Corunna Conglomerate|42738|6|Mentioned|map legend|Mesoproterozoic||||||Mentioned as a probable equivalent to Blue Range beds.||30-JUL-21
27751|Corunna Conglomerate|42934|5|Briefly described|p520 Fig.1|||Intruded by Charleston Granite.||||||12-JAN-10
27751|Corunna Conglomerate|43049|6|Mentioned|p17|||||||||
27751|Corunna Conglomerate|43052|3|Fully described|p124|||Of Gawler Range Volcanics. Age between 1740 and 1585 Ma.||||||04-MAR-09
27751|Corunna Conglomerate|43053|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Sandstone, talus breccia, conglomerate, siltstone.||||||26-MAY-05
27751|Corunna Conglomerate|43141|6|Mentioned|p63,Fig.1|||||||||
27751|Corunna Conglomerate|43258|5|Briefly described|Map Legend||Mesoproterozoic|||||||
27751|Corunna Conglomerate|43298|5|Briefly described|Map Legend||Mesoproterozoic|||||||
27751|Corunna Conglomerate|43595|5|Briefly described|p354,443||Mesoproterozoic|||||||
27751|Corunna Conglomerate|43634|6|Mentioned|p12|||||||||
27751|Corunna Conglomerate|44660|14|Not recorded|map legend||Carpentarian|Carpentarian, lithology.||||||
27751|Corunna Conglomerate|48894|6|Mentioned|p73|||Age: 1535+/-20 Ma.||||||23-JUL-13
27751|Corunna Conglomerate|50225|6|Mentioned|p407|||||||||07-FEB-11
27751|Corunna Conglomerate|50605|5|Briefly described|p1.1, 8.6|||Geological Province: Gawler Craton and Curnamona Province. Intruded by Hiltaba Supersuite.||||||28-FEB-08
27751|Corunna Conglomerate|60515|6|Mentioned|p116 Fig.1 |||||||||
27751|Corunna Conglomerate|60953|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Sandstone, talus breccia, conglomerate, siltstone.||||||07-NOV-08
27751|Corunna Conglomerate|60954|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Geological Province: Gawler Craton.||||||31-MAY-05
27751|Corunna Conglomerate|61070|6|Mentioned|Map Legend|Paleoproterozoic|Paleoproterozoic|Possibly equivalent to Blue Range beds.||||||12-JAN-10
27751|Corunna Conglomerate|61108|5|Briefly described|map legend|Mesoproterozoic|Mesoproterozoic|Sandstone, talus breccia, conglomerate and siltstone.||||||
27751|Corunna Conglomerate|61307|5|Briefly described|p36 Fig. 17|Mesoproterozoic|Mesoproterozoic|Geological Province: Gawler Craton. See also p39 Fig. 19.||||||
27751|Corunna Conglomerate|61522|5|Briefly described|p5 Fig.1|||Geological Province: Gawler Craton.||||||
27751|Corunna Conglomerate|61556|5|Briefly described|p9-10 Figure, p11|||In Middleback Range, Eyre Peninsula.||||||21-NOV-07
27751|Corunna Conglomerate|62727|5|Briefly described|p11|Paleoproterozoic|Paleoproterozoic|Within the Gawler Range Volcanics. Geological Province: Gawler Craton.||||||07-NOV-08
27751|Corunna Conglomerate|62893|6|Mentioned|Map Legend, p15|Middle Proterozoic|Middle Proterozoic|Probably equivalent to the basal conglomerate of the Blue Range Beds.||||||
27751|Corunna Conglomerate|63020|5|Briefly described|p987 Fig. 8|Mesoproterozoic|Mesoproterozoic|Age: ~1590Ma. Geological Province: Gawler Craton.||||||10-AUG-07
27751|Corunna Conglomerate|64130|5|Briefly described|p1383|||Apparently rift-hosted clastic sequence associated with the Gawler Range Volcanics.||||||
27751|Corunna Conglomerate|64131|5|Briefly described|p1402, p1408, p1409 |||Apparently restricted to S and W of Port Augusta.||||Intruded by and interlayered with the coeval Gawler Range Volcanics.|Immature clastic sequence of conglomerate, siltstone and sandstone.|
27751|Corunna Conglomerate|64135|6|Mentioned|p1504. |||Eastern Eyre Peninsula. Has similarities with the interlayered sedimentary rocks of the Gawler Range Volcanics at Prominent Hill.||||||
27751|Corunna Conglomerate|64722|6|Mentioned|Fig. 5 p.13|Proterozoic|Proterozoic|Of South Australian Craton.||||||
27751|Corunna Conglomerate|64739|6|Mentioned|p264 Fig.1.|||Gawler Craton.||||||
27751|Corunna Conglomerate|64828|5|Briefly described|p1064 Fig. 1|Mesoproterozoic|Mesoproterozoic|Geological province: Gawler Craton.||||||04-MAR-09
27751|Corunna Conglomerate|65220|5|Briefly described|p21-22, Fig.4, p19 Fig.1|Mesoproterozoic|Paleoproterozoic|Lower units are bounded by unconformities, in the style of proximal foreland basins, these folded units are crosscut by Gawler Range Volcanics dykes. Age poorly constrained. Maximum depositional age c. 1740 Ma||||||10-DEC-09
27751|Corunna Conglomerate|65221|5|Briefly described|p28 Fig.3a, p29 Fig.4 |Mesoproterozoic|Mesoproterozoic|Of Gawler Range Volcanics||||||
27751|Corunna Conglomerate|65375|6|Mentioned|p13.|||||||||
27751|Corunna Conglomerate|65376|6|Mentioned|p8 Fig.1.1. |Mesoproterozoic|Mesoproterozoic|||||||
27751|Corunna Conglomerate|65390|5|Briefly described|p23 Fig.3, p26 Tb. 1|Calymmian|Statherian|Olympic Domain, Gawler Craton. Intruded by Charleston Granite. Age of about 1690 - 1590 Ma inferred in Figure 3.||||||
27751|Corunna Conglomerate|65485|6|Mentioned|Fig 1|Mesoproterozoic|Mesoproterozoic|||||||
27751|Corunna Conglomerate|65922|5|Briefly described|p13 Fig.4, p16-17, p29 Fig. 6|Calymmian|Calymmian|Exposed near Mount Allalone. Breccia, conglomerate and pebbly quartzite with minor heavy mineral banding. Over 100 m thick.||||||
27751|Corunna Conglomerate|66302|4|Described|p4 Fig.3, p33, p34, p46, |Statherian|Statherian|Spencer and Olympic Domains, Gawler Craton. May have been emplaced in a proximal foreland basin environment. Ages derived from McAvaney and Reid (2008) and Fraser and Neumann (2010), respectively Both probably U-Pb SHRIMP ages. See also p47, p72, p76 Fig.20.|1746 +/- 9 Ma  to 1659 +/- 7 Ma both max dep||Includes the Red Conglomerate Member.|Unconformably overlies the Moonabie Formation and McGregor Volcanics. Intruded by the Charleston Granite.|Unmetamorphosed fluvial to shallow marine conglomerates, sandstones and siltstones.|28-OCT-22
27751|Corunna Conglomerate|67027|5|Briefly described|p349, p351 Table 1.|Mesoproterozoic|Mesoproterozoic|Suggested correlative of Blue Range Beds.||||Intruded by Charleston Granite.|Talus breccia, medium-grained sandstone, conglomerate, local siltstone.|
27751|Corunna Conglomerate|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Southern Gawler Craton. Appears as Upper and Lower Corunna, with a ~10 m.y. separation.|1590 +/- 7 Ma (upper part).|||||
27751|Corunna Conglomerate|67536|5|Briefly described|Map Legend|Calymmian|Statherian|Gawler Craton.|ca. 1587 +/- 15 Ma (tuff)||||Sandstone, conglomerate, siltstone, breccia; includes tuff.|
27751|Corunna Conglomerate|67721|5|Briefly described|p37|Statherian|Statherian|Contains iron ore pebble conglomerates.|c. 1700 Ma|||||
27751|Corunna Conglomerate|67900|6|Mentioned|p32|||Daly et al. (1998). Gawler Craton.||||||
27751|Corunna Conglomerate|68131|5|Briefly described|p2 Fig.1|Mesoproterozoic|Mesoproterozoic||||||Conglomerate, sandstone and siltstone.|
27751|Corunna Conglomerate|68158|5|Briefly described|p4-5, p16|||Contains clasts of Moonabie Formation and Middleback Subgroup jaspilite.|~1750-1680 Ma.|||Unconformably overlies Moonabie Formation and ?Wandearah Metasiltstone. Is intruded by Hiltaba Suite.|White or red conglomerate, polymict conglomerate, green sandstone, dolomite, dark grey laminated glauconitic siltstone and shale, tuffaceous sandstone. Basal volcaniclastic lithic sandstone.|
27751|Corunna Conglomerate|68208|6|Mentioned|p32 Fig.3, p34 Fig.5|Mesoproterozoic|Mesoproterozoic|||||||
27751|Corunna Conglomerate|69004|6|Mentioned|p18|||Gawler Craton.||||||
27751|Corunna Conglomerate|69649|6|Mentioned|p6 Fig.4,|||||||||
27751|Corunna Conglomerate|69666|6|Mentioned|p27 Fig.3|Mesoproterozoic|Mesoproterozoic|||||||
27751|Corunna Conglomerate|70334|5|Briefly described|p75|||Fluvial sediments folded in a gentle N-NW trending syncline occurring on ROOPENA and UNO (Lemon, 1972, Morgan, 2007). Deposited after the Kimban Orogeny (maximum depositional age 1690+\-7 Ma; Fraser and Neumann, 2010), suggesting folding may be related to Kararan Orogeny.||||||
27751|Corunna Conglomerate|70405|6|Mentioned|p12 figure 4|Paleoproterozoic|Paleoproterozoic||1650 Ma|||||
27751|Corunna Conglomerate|70659|5|Briefly described|p4-5, p10|Palaeoproterozoic|Palaeoproterozoic|Northern Eyre Peninsula. Previously thought to be synchronous with Gawler Range Volcanics. Folded during Kararan Orogeny.|||||Fluvial-lacustrine succession.|
27751|Corunna Conglomerate|70721|6|Mentioned|p63-p64|Paleoproterozoic|Paleoproterozoic|Fluvial and colluvial sediments.|c.1680 Ma (max dep)|||||
27751|Corunna Conglomerate|70816|5|Briefly described|p3-4||Statherian|Gawler Ranges region. Fluvial and colluvial sediments deposited after 1680 Ma. (Fraser and Neumann, 2010; McAvaney and Reid, 2008)||||Underlain by Paleoproterozoic sequence comprising Myola Volcanics, Broadview Schist and Top Top Granite.||30-MAY-19
27751|Corunna Conglomerate|70948|5|Briefly described|p974, 975||Statherian|Geological province: Gawler Craton. Fluvial and colluvial sediments.|<1680 Ma.|||||
27751|Corunna Conglomerate|71037|6|Mentioned|p21 Fig.1|Paleoproterozoic|Paleoproterozoic|Shown only on 'Outcropping geology and mineral deposits of northern Eyre Peninsula' map p21 Fig.1.||||Shown as younger than Tunkillia Suite and older than St Peter Suite.|Conglomerate.|
27751|Corunna Conglomerate|71129|5|Briefly described|p17-18,35,64,89,97,205-206|Statherian|Statherian|Geological Province: Cleve-Coulta and Spencer domains, Gawler Craton. Experienced open north-trending folding during Kararan Orogeny ?c. 1610-1590 Ma. Maximum depositional age of 1680+\-7 Ma (Fraser and Neumann, 2010), therefore post-dating c. 1740-1690 Ma Kimban Orogeny. Intruded, and overlain by Gawler Range Volcanics.|<1680 Ma|||Overlain by Spearfelt Rhyodacite. Intruded by Gawler Range Volcanics.||
27751|Corunna Conglomerate|71235|3|Fully described|p1-p9, p11, p14, p19, p22|Mesoproterozoic|Mesoproterozoic|The type locality (never formally defined) is the Corunna Range 4km north of Iron Knob. Stratigraphy of this unit was first described by Lemon (1972) and was refined by Weste (1996). Fluvial to shallow marine sediments. Hosts epithermal style Au-Ag-Pb-Zn mineralisation. Intersected by drillholes PD 63 and PD 30. Potentially a host for unconformity related uranium deposits. A date of 1587 +/- 15 Ma is derived from a tuff interbedded with this unit by Johnson (1993) and is interpreted to suggest that this unit is synchronous with the Gawler Range Volcanics. Intruded by the Gawler Range Volcanics. Equivalent to the Blue Range Beds.|c. 1690-1590 Ma||Includes the Iron Princess beds, Red Conglomerate Member, Cowleds Member, Nilgenee Member.|Overlies (locally unconformably) the Burkitt Granite and Moonabie Formation. Overlies the Middleback Subgroup. Unconformably overlies the Hutchison Group and the Broadview Schist.|Conglomerates, dolomite, sandstones and carbonaceous and chloritic siltstones.|
27751|Corunna Conglomerate|71317|5|Briefly described|p15-p16|Palaeoproterozoic|Palaeoproterozoic|Cleve-Coulta and Spencer Domains, Gawler Craton.||||||
27751|Corunna Conglomerate|71322|5|Briefly described|p103|Mesoproterozoic|Mesoproterozoic|Northern Eyre Peninsula.||||||
27751|Corunna Conglomerate|71413|6|Mentioned|p32 Fig 2|||Geological province: Gawler Craton. ||||||
27751|Corunna Conglomerate|71559|6|Mentioned|p15 Fig 1, p16 Fig 2|Paleoproterozoic|Paleoproterozoic|Geological province: Gawler Craton.||||||
27751|Corunna Conglomerate|71712|5|Briefly described|p410 Fig 1, p411|Calymmian|Calymmian|||||Deposited contemporaneously with Gawler Range Volcanics. Possible correlative to Roopena Basalt.|Conglomerate, quarz sandstone, carbonaceous shale and felsic volcanics.|
27751|Corunna Conglomerate|71859|5|Briefly described|p3-p6, p18|Paleoproterozoic|Paleoproterozoic|Cleve and Coulta domains, southern Gawler Craton.|c. 1680 Ma (McAvaney & Reid, 2008)||||Fluvial and alluvial sediments.|
27751|Corunna Conglomerate|71862|5|Briefly described|p3-p4, p7, p52, p54|Paleoproterozoic|Paleoproterozoic|Deposited on the Eyre Peninsula.|c. 1680 (McAveny and Reid, 2008)|||Unconformably overlies the Burkitt Granite (Moola Suite) and the Peter Pan Supersuite.|Fluvial and alluvial sediments including conglomerate.|
27751|Corunna Conglomerate|72058|6|Mentioned|p171|||Middleback Ranges, Gawler Craton.|~1740-1587 Ma|||||
27751|Corunna Conglomerate|72090|4|Described|p1, p10, p14, p17|||Gawler Craton. Hosts epithermal Au-Ag mineralisation at Parkinsons Dam along the south-east Gawler Ranges. See also p86-p87, p112, p115, p120.||||Intruded by the Pennas Granite.|Fine- to medium-grained metasandstone, minor metasiltstone, massive quartzite, variably mylonitised calc-silicate rock, psammite, minor breccia.|
27751|Corunna Conglomerate|72237|6|Mentioned|p28|||Geological province: Gawler Craton. Of Roopena Basin.||||||
27751|Corunna Conglomerate|72461|6|Mentioned|p6|||Gawler Craton.|c. 1610 Ma|||||
27751|Corunna Conglomerate|72462|6|Mentioned|p3|Paleoproterozoic|Paleoproterozoic|Gawler Craton.||||||
27751|Corunna Conglomerate|72463|6|Mentioned|p2, p6|Mesoproterozoic|Mesoproterozoic|Hosts epithermal veins at Parkinson Dam Au-Ag prospect. May be overlain by Gawler Range Volcanics.||||Underlain by Broadview Schist.||
27751|Corunna Conglomerate|72484|6|Mentioned|p3|||Eyre Peninsula, Gawler Craton.|~1740-1587 Ma.|||||
27751|Corunna Conglomerate|73026|5|Briefly described|p9, p11|Mesoproterozoic|Mesoproterozoic|||||||
27751|Corunna Conglomerate|73027|6|Mentioned|p9,, p12 fig 1.5,|Mesoproterozoic|Mesoproterozoic|||||||
27751|Corunna Conglomerate|73103|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic||||Nilgenee, Cowleds Members.||Conglomerate, boulder and pebble; minor sandstone, off-white to purple.|
27751|Corunna Conglomerate|73104|5|Briefly described|p2-7, p11-12, p15, p19-20, p24, p51|Statherian|Statherian|Cleve and Spencer Domains. Predominantly exposed in the Corunna and Uno ranges. Correlated with a metasedimentary succession exposed at Mount Allalone and intersected in drillhole MSDP13 based on detrital zircon spectra. This correlated succession may have been sourced locally from Nummee Granodiorite (Tunkillia Suite) and Peter Pan Supersuite rocks. Inferred basement rock of the Mount Double area. In the Mount Double area, it fills a north-trending graben bounded by the Allalone Fault. [Article includes locality/outcrop and petrographic description from Mount Allalone].|c. 1650 Ma, <1660 Ma >1595 Ma||||Conglomerate, sandstone, siltstone and dolomite.|
27751|Corunna Conglomerate|73110|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Ten facies are mapped separately.|||||Conglomerate, boulder and pebble; minor sandstone, off-white to purple.|
27751|Corunna Conglomerate|73130|6|Mentioned|[poster] Fig.1|Mesoproterozoic|Mesoproterozoic|||||||28-OCT-22
27751|Corunna Conglomerate|73162|6|Mentioned|p451|Statherian|Statherian|northern Eyre Peninsula. Younger than ca 1660 Ma, deformed prior to eruption of the Gawler Range Volcanics. Originally correlated with Fresh Well Formation but now considered distinctly older and defined as distinct stratigraphic units.|younger than ca 1660 Ma||||Alluvial to fluvial succession.|
27751|Corunna Conglomerate|73234|6|Mentioned|p19|Statherian|Statherian|Exposed in the Baxter and Uno ranges to the west of Six Mile Hill. Contains a prominent 1690-1660 Ma zircon population, but also a prominent 1750-1720 Ma population (Fraser and Neumann, 2010).|c. 1650 Ma|||||
27751|Corunna Conglomerate|73235|6|Mentioned|p53, p60-61, p64|Statherian[?]|Statherian|Gawler Craton. Spencer, Cleve, Coulta, and Gawler Range Volcanic regions. Hosts Parkinson Dam epithermal gold mineralisation in the Southern Gawler Range Volcanics mineral field of the Kararan (Gawler Range Volcanics) gold mineral system.|<1680 Ma|||||
29934|Cotabena Formation|43052|5|Briefly described|Table 2.1 p27||Early Eocene|Torrens Basin||||||
29934|Cotabena Formation|44133|5|Briefly described|p187|Early Oligocene|Early Eocene|Geological Province: Torrens Basin. Formerly referred to as 'Wilkatana Formation'. Overlain by Neuroodla Formation.||||||
29934|Cotabena Formation|60959|5|Briefly described|Map Legend|Eocene|Eocene|Fluvio-lacustrine, partly carbonaceous, fine to coarse grained sand, silt, clay and lignite.||||||
23514|Coulta Granodiorite|22489|6|Mentioned|p14|Archean|Archean|||||||07-NOV-08
23514|Coulta Granodiorite|22629|5|Briefly described|p148|||||||||
23514|Coulta Granodiorite|23317|5|Briefly described|p384|Paleoproterozoic||Age: 2512+/-2Ma, 2514+/-7Ma; and  2520+/-9Ma (SHRIMP)||||||07-NOV-08
23514|Coulta Granodiorite|23491|5|Briefly described|p20 Fig. 4||Archean|Intruded by Kiana Granite. Age: ~2540 Ma.||||||07-NOV-08
23514|Coulta Granodiorite|39802|6|Mentioned|Map legend|Archean|Archean|||||||07-NOV-08
23514|Coulta Granodiorite|40448|5|Briefly described|Table 2|||||||||
23514|Coulta Granodiorite|40644|6|Mentioned|p120|||Of Fanning (in Parker et al 1981). Included in the Dutton suite as presented in this paper. Intruded by Kiana Granite. Geological province: Gawler Craton.||||||13-AUG-08
23514|Coulta Granodiorite|41667|5|Briefly described|p2|||||||||
23514|Coulta Granodiorite|43052|5|Briefly described|p38,Table 3.1|||Of Dutton Suite.||||||21-OCT-08
23514|Coulta Granodiorite|50605|5|Briefly described|p4.2, 8.7|||Geological Province: Gawler Craton & Curnamona Province. Of the Dutton Suite (Sleaford Complex).||||||
23514|Coulta Granodiorite|61070|5|Briefly described|Map Legend|Proterozoic|Archean|Of the Dutton Suite. Grey, foliated medium to coarse-grained granodiorite with abundant, variably assimilated amphibolite xenoliths. Emplacement age: 2517 +/- 14Ma (U-Pb Zircon). Geological Province: Gawler Craton.||||||12-JAN-10
23514|Coulta Granodiorite|63223|5|Briefly described|p16, p19|||Of the Dutton Suite. Intruded parts of the Sleaford Complex. Geological Province: Gawler Craton.||||||30-APR-07
23514|Coulta Granodiorite|64313|5|Briefly described|p450 Fig. 1|Archean|Archean|Age: 2519+/-8Ma (U-Pb zircon). Geological province: Gawler Craton.||||||09-FEB-10
23514|Coulta Granodiorite|64722|6|Mentioned|p12|Neoarchean|Neoarchean|Of (or intrudes?) Sleaford Complex, Gawler Province. Emplaced as part of igneous activity between 2650 and 2500 Ma.||||||
23514|Coulta Granodiorite|64828|5|Briefly described|p1065 Fig. 2|||Of the Dutton Suite. Included in the Sleaford Complex also. Age: 2519+/-8Ma (Fanning et al 2007).||||||04-MAR-09
23514|Coulta Granodiorite|65376|5|Briefly described|p15.|||Early-formed intrusion.|2519 +/- 8 Ma.|Unit in Dutton Suite.||Intruded by Kiana Granite.||
23514|Coulta Granodiorite|65390|5|Briefly described|p19|Neoarchean|Neoarchean|Of Dutton Suite, Gawler Craton. Has a U-Pb zircon age of 2517 +/- 14 Ma (Fanning, 1997).||||||
23514|Coulta Granodiorite|66302|6|Mentioned|p11, p12, p14, p61, p61 Fig.14, p85|Neoarchean|Neoarchean|Christie and Wilgena Domains, Gawler Craton. Interpreted to have its origin in the same magmatic system as the Glenloth Granite, Devils Playground and Hall Bay Volcanics.|2519 +/- 8 Ma (SHRIMP U-Pb, Fanning et al, 2007)|Dutton Suite||||
23514|Coulta Granodiorite|67058|5|Briefly described|p492.|Archean|Archean|Contains significant negative Eu anomalies: may be a source for the Eba Formation.|c.2517 Ma.|||||
23514|Coulta Granodiorite|68128|6|Mentioned|p7|||Gawler Craton. SHRIMP age is dervied from Swain et al, 2005.|2517 +/- 7 Ma (SHRIMP U-Pb)|||||
23514|Coulta Granodiorite|68208|6|Mentioned|p31 Fig.2, p39|Neoarchean|Neoarchean||Crystallisation age ~2520 Ma|Of Sleaford Complex||||
23514|Coulta Granodiorite|69554|6|Mentioned|p139 Fig.10|||Gawler Craton.|2510 Ma (Howard et al., 2009).|||||
23514|Coulta Granodiorite|71859|5|Briefly described|p7, p9-p10, p16, p28|||Southern Eyre Peninsula.|c. 2520 Ma|Dutton Suite||Intrudes the Hall Bay Volcanics.|Medium- to coarse-grained, foliated grey granodiorite with mafic xenoliths.|04-APR-23
23514|Coulta Granodiorite|73061|6|Mentioned|p1076 Fig.5, p1077|||Gawler Craton.||||||
75707|Coulthard Suite|67540|3|Fully described|p25, p26 Fig.1; p32,36 Tb.2,3|Calymmian|Calymmian|Named after Coulthards Lookout, Mount Painter region. Several age references cited. Curnamona Province, Moolawatana Domain. Tb.1 has age range as 1600-c.1570 Ma. Maximum age given here is by LA-ICP-MS (Kromkhun 2008, 2010); the minimum is by U-Pb ion microprobe (Fanning, 1995).|1590 +/- 5 Ma to 1569 +/- 14 Ma.|Of the Ninnerie Supersuite.|Includes Mount Neill Granite, Nooldoonooldoona Trondhjemite, Box Bore Granite.|Faulted against and/or intrudes Radium Creek Metamorphics.|Varies from undeformed, fine-to coarse-grained granites to highly deformed, pink-red, coarse-grained, megacrystic granitic gneiss or rapakivi granites; also a sodic variety characterised by blue quartz. A-type.|08-FEB-16
75707|Coulthard Suite|67900|6|Mentioned|p19|||Mount Painter Inlier, Curnamona Province.||Ninnerie Supersuite.|||Granites and volcanic rocks.|
75707|Coulthard Suite|68715|6|Mentioned|p32 Fig.6||||||||Granitoids.|07-APR-17
75707|Coulthard Suite|69562|5|Briefly described|p670 Tb.5||||c.1585-1575 Ma.||Includes Box Bore and Mount Neill Granites.|||
75707|Coulthard Suite|69650|2|Defined|p4 Tb.1, p2, p8, p11, p13, p45, p57-71|Calymmian|Calymmian|See also p73-74. Moolawatana Domain, Curnamona Province. Named after Coulthards Lookout near Arkaroola. See individual Members for type sections. Geochemistry detailed.|~1600-1570 Ma.|Unit in Ninnerie Supersuite.|Includes Box Bore Granite, Nooldoonooldoona Trondhjemite, Mount Neill Granite.|Faulted against or intrudes Radium Creek Metamorphics.|Variety of granites: undeformed, fine- to coarse-grained granite; highly-deformed, pink-red, coarse-grained,megacrystic granitic gneiss or rapakivi granites; sodic granite with blue quartz. A-type.|25-NOV-22
75707|Coulthard Suite|70383|5|Briefly described|p44|Mesoproterozoic|Mesoproterozoic|Mount Painter Inlier.|Between c.1580 Ma and 1550 Ma.|||Intrudes Radium Creek Group.|Granites and granodiorites.|
75707|Coulthard Suite|70384|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|||Ninnerie Supersuite.|Box Bore, Mount Neill Granites; Nooldoonooldoona Trondhjemite.||Granite, trondhjemite, granitic gneiss.|
75707|Coulthard Suite|70658|5|Briefly described|p33, 35|Mesoproterozoic|Mesoproterozoic|Occurs only in the Moolawatana Domain, Mount Painter Province.|c.1590 - c.1575 Ma.|Ninnerie Supersuite.|Box Bore, Mount Neill Granites; Nooldoonooldoona Trondhjemite.|Is overlain by Benagerie Volcanic Suite.|A-type, compositionally variable granites. Undeformed to highly deformed. Fine- to coarse-grained granites, some with rapakivi texture.|
75707|Coulthard Suite|71341|6|Mentioned|p179 fig 1|Mesoproterozoic|Mesoproterozoic||ca. 1585-1555 Ma|||||
75707|Coulthard Suite|73251|6|Mentioned|p37|early Mesoproterozoic|early Mesoproterozoic|||||||
31508|Cowirra Clay Member|23226|2|Defined|p896||Longfordian|Very similar lithology to Overland Corner Clay Member of the Cadell Formation and deposition in a similar environment to the Geera Clay. Of Finniss Formation.||||||
31508|Cowirra Clay Member|63460|5|Briefly described|p847|Early Miocene|Early Miocene|Of Finniss Formation. Geological province: Murray Basin.||||||
31508|Cowirra Clay Member|64237|5|Briefly described|p19 Fig. 2b|Early Miocene|Early Miocene|Of the Finniss Formation (Murray Group). Originally introduced as a new member with the stratigraphic revision of the Murray Group up to Murray Supergroup by Lukasic and James (1998), but retained when Murray Group was reinstated.||||||
23516|Cowleds Member|23719|4|Described|p23|Mesoproterozoic|Mesoproterozoic|See also page 22 table 6. Of Corunna Conglomerate. Overlying unit Blue Range Beds.  Underlying unit Nilgenee Member. Geological Province: Gawler Craton. Max. thickness 500 m.||||||
23516|Cowleds Member|37621|6|Mentioned|p15|||||||||
23516|Cowleds Member|39349|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
23516|Cowleds Member|40448|6|Mentioned|p36|||||||||
23516|Cowleds Member|43052|5|Briefly described|p125|||of Corunna Conglomerate||||||
23516|Cowleds Member|71235|6|Mentioned|p8-p9|||||Corunna Conglomerate||Intertongues with the Nilgenee Member.|Talus breccia.|
23516|Cowleds Member|73103|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|||Corunna Conglomerate.|||Breccia, massive talus.|
29204|Cox Sandstone Member|22510|5|Briefly described|table1, p38|||Of the Tarcowie Siltstone.  Age: Marinoan||||||13-OCT-04
29204|Cox Sandstone Member|22631|6|Mentioned|p178|||Age: Marianoan||||||
29204|Cox Sandstone Member|41405|3|Fully described|p175|||Also mentioned as "Cox Sandstone" on p175.||||||19-FEB-08
29204|Cox Sandstone Member|41500|4|Described|p80|||||||||
29204|Cox Sandstone Member|42098|5|Briefly described|p54|||||||||
29204|Cox Sandstone Member|42109|2|Defined|p18|Marinoan||||||||
29204|Cox Sandstone Member|42222|6|Mentioned|Table 1 P4|||||||||
29204|Cox Sandstone Member|42542|5|Briefly described|Fig.2a P11|||||||||
29204|Cox Sandstone Member|42720|5|Briefly described|map legend|Marinoan||||||||
29204|Cox Sandstone Member|42813|5|Briefly described|p20|||of Tarcowie Siltstone||||||
29204|Cox Sandstone Member|42882|5|Briefly described|p10, Fig.5 p8|||of Tarcowie Siltstone||||||
29204|Cox Sandstone Member|43052|5|Briefly described|p189,Table 6.1|||of Tarcowie Siltstone||||||
29204|Cox Sandstone Member|61732|5|Briefly described|p28 Fig. 13|Marinoan|Marinoan|Of the Sutherland Formation (Upalinna Subgroup, Umberatana Group). Geological Province: Adelaide Rift Complex.||||||07-FEB-11
29204|Cox Sandstone Member|65925|5|Briefly described|Appendix 2.||||||||Sandstone, coarse-grained; sandstone medium- to fine-grained, with siltstone.|
29204|Cox Sandstone Member|70334|5|Briefly described|p90|Neoproterozoic|Neoproterozoic|Geological province: Gawler Craton. Of Adelaide Geosyncline and Stuart Shelf. Contains structurally controlled quartz-carbonate veins and stock work zones with potential to host Au mineralisation.||Unit of Tarcowie Limestone.||||
29204|Cox Sandstone Member|70407|5|Briefly described|p103 Fig 2|Neoproterozoic|Neoproterozoic|Age: Marinoan.||Of Tarcowie Siltstone.||||
29204|Cox Sandstone Member|73226|6|Mentioned|p3|||||||||
29204|Cox Sandstone Member|74367|6|Mentioned|p7 Fig.6|||||Upalinna Subgroup||||
34784|Cradock Quartzite Member|22889|5|Briefly described|p39|Adelaidean|Adelaidean|The Cradock Quartzite Member superseds the former Cradock Quartzite as the unit has been downgraded from formation to member status, see p 39 for details.||||||
34784|Cradock Quartzite Member|62724|5|Briefly described|p17 Fig. 4, p22|Torrensian|Torrensian|Of Saddleworth Formation (Bungarider Subgroup, Burra Group). Geological Province: Curnamona Province.||||||07-FEB-11
73284|Crayfish Supersequence|63134|2|Defined|101|||||||||
73284|Crayfish Supersequence|63269|5|Briefly described|p605, p609, p616, p618, p622-624|Early Cretaceous|Early Cretaceous|Otway Basin. Oil-source correlation.|||Casterton Formation and Crayfish Subgroup.|Is overlain by Eumeralla Supersequence.||
73284|Crayfish Supersequence|69297|6|Mentioned|p77, p80, p81, p82, p96-p100, p110|Lower Cretaceous|Upper Jurassic|Nelson Sub-basin of the Otway Basin. Deposited in a fluvial or lacustrine environment. Interpreted from seismic data. ||||||
73284|Crayfish Supersequence|69651|5|Briefly described|p6, p10, p12-15, p17-19, p23, p25, p31||Early Cretaceous|See also p36-38, p40, p42-44, p47, p49-50. Krassay et al. (2004). Otway Basin. Part of the Otway Supergroup. Potential source rocks. Fluvial to lacustrine deposits. Modelling diagrams.||||Is overlain by Eumeralla Supersequence.|Argillaceous sandstone with interbedded claystone.|
73284|Crayfish Supersequence|70077|5|Briefly described|Nelson:p1. Regional: Fig.4; p3-4, p6, p9|Early Cretaceous|Early Cretaceous|Non-marine, fluvio-lacustrine deposits (shales and coals). A thick growth wedge in the ENE-trending Nerita Trough. Good potential source rocks.||||||
73284|Crayfish Supersequence|70078|6|Mentioned|Regional: Fig.4; p3-4|Early Cretaceous|Early Cretaceous|Hosts Austral 1 and part of Austral 2 petroleum systems.||||||
73284|Crayfish Supersequence|70880|5|Briefly described|p75-77, 82-83|Barremian|Tithonian|Otway Basin. Australia-Antarctica rifting produced E-W to NW-SE striking faults bounding horst-and-graben structures. Syn-rift deposition. Maximum thicknesses up to 5000m in northern onshore Basin.||||Is overlain unconformably by Eumeralla Supersequence.|Contains organic-rich mudstones, sandstones and some basalts.|
73284|Crayfish Supersequence|71266|5|Briefly described|p613-615, p617, p620, p622 Fig.10|Barremian|Tithonian|Contains the oldest known stratigraphic units in the Otway Basin. Syn-rift deposition. Up to 5000m thick in the northern, onshore part of the Basin. Affected by faults; their growth is discussed in great detail.||||Is overlain by Eumeralla Supersequence.|Organic-rich mudstones, sandstones and basalts.|
69827|Crocker Well Suite|66302|5|Briefly described|p50|||Olary Domain, Curnamona Province. |1580 to 1568 Ma (Ludwig and Cooper, 1984)|Ninnerie Supersuite|||Biotite-rich, sodic granites including trondhjemite, alaskite and mafic I-type granodiorites and diorite.|
69827|Crocker Well Suite|66518|6|Mentioned|p19 Fig.4.|Mesoproterozoic|Mesoproterozoic|Curnamona Province.||Unit in Ninnerie Supersuite.||||
69827|Crocker Well Suite|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Olary Domain.|1579 +/- 2 Ma.|||||
69827|Crocker Well Suite|67540|3|Fully described|p25-28, p36 Tb.3, p37, p38 Fig.2|Calymmian|Calymmian|Type Locality: Ninnerie Hill and Crockers Original Mine. Curnamona Province, Western Olary Domain. Definition reference: this article and Fricke and Hore (2011). Ages from Ludwig and Cooper (1984). High-K, high Th radiometric signature. S-type.|1580+/-21 Ma-1568+/-2 Ma (conventional U-Pb).|Of the Ninnerie Supersuite.|Includes Mount Victoria Granite, Mindamereeka Trondhjemite.|Intrudes the host Willyama Supergroup sediments. Intermingled with the Windamerta Diorite.|Biotite-bearing monzogranites and sodic granites including trondhjemites and alaskites. S-type and I-type granites.|25-NOV-22
69827|Crocker Well Suite|67653|4|Described|p2-5,11,13,15,28-29|Calymmian|Calymmian|Geological province: Curnamona Province. Age of magmatism from Ludwig and Cooper, 1984; pooled zircon U-Pb age of 1579.2+\-1.5 Ma for two samples of unmineralised leucoadamellite and adamellite. Comprises three groups of geochemically distinct igneous rocks, of which most of the Crocker Well Suite belongs to the main granitic group, with secondary components of dioritic and granodioritic rocks, and high-Na granitic rocks. High-Na rocks are weakly related to main granitic suite, and are associated with U-Th mineralisation.|1579.2+\-1.5 Ma|||||
69827|Crocker Well Suite|67900|6|Mentioned|p19|||Curnamona Province.||Ninnerie Supersuite.|||Sodic and muscovite-biotite and biotite-only granites.|
69827|Crocker Well Suite|68126|5|Briefly described|p3, p5-7|||Olary Domain, Curnamona Province. Several age determinations by Ludwig and Cooper (1984) listed, almost all between c.1568 - c.1580 Ma.|1579+/-3 Ma.|Ninnerie Supersuite.|||Sodic and biotite-only granites.|
69827|Crocker Well Suite|68715|6|Mentioned|p32 Fig.6||||||||Granitoids.|07-APR-17
69827|Crocker Well Suite|69213|6|Mentioned|p34||||||||Granitoids.|
69827|Crocker Well Suite|69562|5|Briefly described|p669, p671 Tb.5, p674 Fig.6|||S Lake Frome region.|c.1580 Ma.|Unit in Ninnerie Supersuite.|Includes Mindamereeka Trondhjemite and Mount Victoria Granite.|||
69827|Crocker Well Suite|69650|2|Defined|p4 Tb.1, p2, p5 Tb.2, p10 Tb.3, p12, p16|Calymmian|Calymmian|See also p20-26, p29, p34, p38, p45. Western Olary Domain, Curnamona Province. Named after Crocker Well Mine, 49 km NW of Manna Hill. Also has appeared as Crockers Well Suite. Type locality:  Mount Victoria, GDA 94, zone 54, 394125 mE, 6463662 mN (Fig. 5) and Crockers Original Mine (GDA 94 386846 mE, 6457573 mN). Extreme enrichment in U and Th. Geochronology results, geochemistry detailed. Intimate mingling relationships with Windamerta Diorite.|c.1580-1568 Ma.|Unit in Ninnerie Supersuite.|Includes host Willyama Supergroup, Mindamereeka Trondhjemite and Mount Victoria Granite.||Biotite-bearing monzogranites and sodic granites including trondhjemites and alaskites. S-type and I-type.|25-NOV-22
69827|Crocker Well Suite|70339|5|Briefly described|map legend|Mesoproterozoic|Mesoproterozoic||U-Pb ages 1580-1568 Ma.|Ninnerie Supersuite.|||Sodic or biotite granitoids: alaskite, leucocratic phlogopite trondhjemite and granodiorite.|02-FEB-16
69827|Crocker Well Suite|70405|5|Briefly described|p47|Mesoproterozoic|Mesoproterozoic|Doesnt occur in mapping area.||Ninnerie Supersuite|||Uraniferous biotite I and S type granites, with sodic varieties such as trondhjemite and alaskite. Strong Th and U responses.|
69827|Crocker Well Suite|70657|5|Briefly described|p48-49|Calymmian|Calymmian|Crocker Well - Billeroo region, Olary Domain. Conventional zircon U-Pb age.|1579 +/- 2 Ma (Ludwig and Cooper, 1984).||||Biotite and sodic granites, alaskites and related intermediate rocks.|
69827|Crocker Well Suite|70658|5|Briefly described|p33-34, 36|Mesoproterozoic|Mesoproterozoic|Restricted to the Crocker Well region, Plumbago Inlier, Olary Domain, Curnamona Province. Geochemistry briefly described.|~1580-1568 Ma.|Ninnerie Supersuite.|Mindamereeka Trondhjemite, Mount Victoria Granite.||Metaluminous, compositionally variable granites. Range from biotite-only to biotite-muscovite granites and a group of distinct sodic granites (trondhjemites) and alaskites. S- and I-types.|
69827|Crocker Well Suite|72454|4|Described|p2 Fig.2, p3,p7-13, p18,p21-22,p24-26,|Mesoproterozoic|Mesoproterozoic|Part of the Olary Domain where they represent the most extensive outcropping granites there. Geochronology by conventional U-Pb Ludwig and Cooper (1984). Informally subdivided on p25 Table 4 into monzogranites, trondhjemites, alaskites, diorites, where geochemistry summarised. Sodix granites comprise leucocratic phlogopite trondhjemites, adamellites and alaskites. Granites display co-magmatic field relationships with each other and more mafic granodiorite to diorite series in the Crocker Well region. Distinct from the Bimbowrie Suite on standard RGB K-U-Th radiometric imagery. Associated with U and Th mineralisation localised along fracture zones as disseminated fissue fillings, veins, stockworks and phlogopitic brecciia-hosted thorian brannerite. See also p29,32,34,35, 39-40,43-44, 46-54, 60-63, 81-81  p9 Fig.7-8,|1579 +/-3 to 1568 +/- 2 Ma.|Ninnerie Supersuite||Coeval with Bimbowrie Suite.|Includes sodic to biotite only granites and granodiorites to diorites and monzogranite trondhjemite, sodic granite and alaskite counterparts. Granites are weakly- to non-foliated, equigranular to strongly porphyritic, medium to coarse-grained.|09-SEP-20
69827|Crocker Well Suite|72949|6|Mentioned|p36|Calymmian|Calymmian|Curnamona Province. Broken Hill / Olary Blocks.|1580-1568 Ma|||||
69827|Crocker Well Suite|73251|6|Mentioned|p36|Calymmian|Calymmian|Curnamona Province. Includes uraniferous crystalline rock.|c. 1590 Ma|Ninnerie Supersuite||||
26505|Crown Point Formation|13516|6|Mentioned|p147, fig 5|Early Permian|Early Permian|From Pedirka Basin||||||
26505|Crown Point Formation|22566|5|Briefly described|p79|Early Permian|Late Carboniferous|Of the Finke Group.||||||08-AUG-06
26505|Crown Point Formation|22804|6|Mentioned|p455||Early Permian|||||||
26505|Crown Point Formation|22824|6|Mentioned|p537||Early Permian|Geological Province - Pedirka Basin.||||||
26505|Crown Point Formation|22826|4|Described|p576|Early Permian|Early Permian|Geological Province - Pedirka Basin.||||||
26505|Crown Point Formation|22883|6|Mentioned|P29|Early Permian|Late Carboniferous|Overlying unit is Purni Formation.||||||08-AUG-06
26505|Crown Point Formation|23982|6|Mentioned|p96 Appendix 13|||Geological Province: Great Artesian Basin.||||||
26505|Crown Point Formation|24204|5|Briefly described|p262, 263 Fig.4, p266 Fig.7|Early Permian|Late Carboniferous|Geological Province: Pedirka Basin.||||||
26505|Crown Point Formation|29442|6|Mentioned|p103|||||||||
26505|Crown Point Formation|29591|6|Mentioned|p82|||||||||
26505|Crown Point Formation|30340|6|Mentioned|p2519|||Lithology||||||
26505|Crown Point Formation|30341|4|Described|p120|||Permian age. Pedirka Basin.||||||
26505|Crown Point Formation|30514|6|Mentioned|p100|||Permian age||||||
26505|Crown Point Formation|30544|5|Briefly described|p52|||See also Fig.6 p53.||||||08-AUG-06
26505|Crown Point Formation|30825|6|Mentioned|p37|||||||||
26505|Crown Point Formation|31567|6|Mentioned|p274|||Latest Carb.- early Permian. Unconformable on Finke Gp.||||||
26505|Crown Point Formation|32640|6|Mentioned|p241|||||||||
26505|Crown Point Formation|33103|6|Mentioned|p25|||||||||
26505|Crown Point Formation|33523|6|Mentioned|p23|||||||||
26505|Crown Point Formation|33824|6|Mentioned|p7|||||||||
26505|Crown Point Formation|33832|6|Mentioned|p7|||Stratigraphy||||||
26505|Crown Point Formation|33844|4|Described|p36|||||||||
26505|Crown Point Formation|33931|6|Mentioned|p9|||L.Perm.||||||
26505|Crown Point Formation|33971|3|Fully described|p32|||||||||
26505|Crown Point Formation|33976|6|Mentioned|p5|||||||||
26505|Crown Point Formation|34111|6|Mentioned|p16|||Permian||||||
26505|Crown Point Formation|34580|4|Described|Table 1|||Permian||||||
26505|Crown Point Formation|35845|6|Mentioned|Fig.25|||||||||
26505|Crown Point Formation|36473|6|Mentioned|Map legend|Permian|Permian|||||||
26505|Crown Point Formation|36733|6|Mentioned|p14|||||||||
26505|Crown Point Formation|36751|6|Mentioned|p489|||||||||
26505|Crown Point Formation|36899|6|Mentioned|p1089|||||||||
26505|Crown Point Formation|36922|6|Mentioned|p188|||||||||
26505|Crown Point Formation|37776|6|Mentioned|Fig.2|||||||||
26505|Crown Point Formation|37855|6|Mentioned|p4|||See also Fig.2.||||||
26505|Crown Point Formation|37917|4|Described|p470|||||||||
26505|Crown Point Formation|39265|6|Mentioned|Fig. 3|||||||||
26505|Crown Point Formation|40637|6|Mentioned|Fig.2|||||||||
26505|Crown Point Formation|40910|5|Briefly described|p15|||||||||
26505|Crown Point Formation|40911|6|Mentioned|Map legend|Permian|Carboniferous|||||||
26505|Crown Point Formation|40925|6|Mentioned|Map legend|Permian|Carboniferous|Carboniferous to Permian||||||
26505|Crown Point Formation|40926|3|Fully described|p12|||Mention Table 1||||||
26505|Crown Point Formation|41063|6|Mentioned|p46|||||||||
26505|Crown Point Formation|41183|6|Mentioned|Fig.3 p308|||||||||
26505|Crown Point Formation|41270|6|Mentioned|p279|||||||||
26505|Crown Point Formation|41491|6|Mentioned|Fig.8|||||||||
26505|Crown Point Formation|41689|6|Mentioned|Table 1|||||||||
26505|Crown Point Formation|42463|6|Mentioned|Fig.4 P171|||||||||
26505|Crown Point Formation|42504|5|Briefly described|p81|||||||||
26505|Crown Point Formation|42547|4|Described|p82|||||||||
26505|Crown Point Formation|42746|5|Briefly described|p3, Fig.2 p4|||Pedirka Basin||||||
26505|Crown Point Formation|42940|5|Briefly described|Plate 2|Permian|Permian|Sandstone, diamictite, shale, siltstone. Age: 290-250Ma.  Geological province: Amadeus Basin.||||||23-JAN-08
26505|Crown Point Formation|43052|5|Briefly described|Table 2.1|||||||||
26505|Crown Point Formation|44133|5|Briefly described|p42, 65 Fig 8.4, 89|Permian|Carboniferous|Geological Province: Pedirka Basin. ||||||
26505|Crown Point Formation|44323|14|Not recorded|map legend||Permian|SG/53-6.||||||
26505|Crown Point Formation|44335|4|Described|p.11||Permian|Table 2. p.10||||||
26505|Crown Point Formation|44336|14|Not recorded|map legend||Permian|SG/53-3.||||||
26505|Crown Point Formation|44342|14|Not recorded|Not recorded|||||||||
26505|Crown Point Formation|44393|4|Described|p.6,8,Tb.1,Fig.1||Early Permian|L. Permian.||||||
26505|Crown Point Formation|44394|14|Not recorded|map legend||Early Permian|Lower Permian.||||||
26505|Crown Point Formation|45041|4|Described|p112|||Permian||||||
26505|Crown Point Formation|45104|6|Mentioned|p30|||||||||
26505|Crown Point Formation|45168|6|Mentioned|p10|||||||||
26505|Crown Point Formation|46849|6|Mentioned|p199|||||||||
26505|Crown Point Formation|48865|2|Defined|p.36||Permian|Fig.4. On many pages. p.21,28,33,34,37,39,41,48,51. Fig.13, Pl.6,11. (G53-6).||||||
26505|Crown Point Formation|48880|14|Not recorded|p.20||Permian|(map).||||||
26505|Crown Point Formation|48890|4|Described|p.53||Permian|||||||
26505|Crown Point Formation|48963|6|Mentioned|Plate 5|||||||||
26505|Crown Point Formation|62376|5|Briefly described|p84|Late Carboniferous|Late Carboniferous|Geological Province: Pedirka Basin.||||||09-FEB-10
26505|Crown Point Formation|64778|6|Mentioned|p13, 15-21, 23|Carboniferous|Carboniferous|Pedirka Basin. Thermal history summarised. Max. palaeotemperature analysis summary. Potential hydrocarbon source rock.|314-285 Ma.|||||
26505|Crown Point Formation|65238|5|Briefly described|p3, p5 Fig. 6, p7 Fig. 8|Late Carboniferous|Late Carboniferous|Geological province: Pedirka Basin. Periglacial deposits - dominantly a glacial succession, comprising diamictite, glacial-fluvial outwash, ripple laminated sandstone and siltstone, together with shale and varved successions. See also p8.||||||09-APR-13
26505|Crown Point Formation|65309|6|Mentioned|p21.|||Pedirka Basin. Useful as an aquifer.||||||
26505|Crown Point Formation|65342|6|Mentioned|p10.|||Pedirka Basin. Max. thickness at least 193 m.||||Overlies Idracowra Sandstone. Is overlain by De Souza Sandstone.||
26505|Crown Point Formation|65489|5|Briefly described|p55, p57-58, p60-61, p63-64, p137-139|Permian|Permian|See also p143, p151. Basal unit in the Pedirka Basin. Perhaps over 600m thick. Has reservoir potential.||||Is overlain by Purni Formation. Equivalent to Merrimelia Formation.|Fluvioglacial and glaciolacustrine sediments.|
26505|Crown Point Formation|67856|6|Mentioned|p348|||Of central Amadeus Basin.||||Correlated with Buck Formation and Ligertwood beds.||
26505|Crown Point Formation|69454|5|Briefly described|p38:1-6,7 Fig.38.6; 38:12-13,14 Fig.38.9|Asselian|Asselian|Wells et al. (1966). The only outcropping strata of the Pedirka Basin. Early Permian. 504m thick in Mount Hammersley-1. Crops out as mesas, buttes and low mounds. Glaciofluvial, glaciolacustrine and periglacial deposits. Sandstones have fair to good reservoir potential.||||Is overlain conformably by, and interfingers with, Tirrawarra Sandstone. Also overlain by Purni Formation. Correlated with Merrimelia, Boorthanna and Kuriyippi Formations.|Conglomerate, diamictite, cross-bedded pebbly and coarse sandstone, ripple-laminated fine sandstone and siltstone, thick claystone-dominated intervals with varvite bands.|12-JUL-16
26505|Crown Point Formation|69457|6|Mentioned|p41:5 Fig.41.4|||||||||12-JUL-16
26505|Crown Point Formation|69673|4|Described|p149, p150, p151, p160, p161 fig 131|Permian|Permian|Greater than 504m thick.||||Conformably overlain by Purni Formation,|Conglomerate, diamictite, cross bedded pebbly and coarse sandstone, ripple laminated fine sandstone and siltstone.|
26505|Crown Point Formation|69946|4|Described|p5-6, p36, p44-48, p51|Asselian|Late Carboniferous|Pedirka Basin. Defined by Wells et al. (1966) to replace the informal Crown Point Series. Type section is at One Tree Point, near Crown Point, NT. Diamictite clasts are derived from early Paleozoic sediments and Musgrave Province. Up to 347m thick.||||Is overlain disconformably by Purni Formation or Stuart Range Formation equivalent. Correlates with Boorthanna and Merrimelia Formations.|Pale grey to buff, very fine- to coarse-grained sandstone with interbeds of medium to dark grey siltstone and diamictite units containing faceted and striated exotic pebbles and cobbles.|
26505|Crown Point Formation|69948|6|Mentioned|Fig.4.18|||Pedirka Basin.||||Is overlain conformably by Stuart Range Formation and (locally) unconformably by Purni Formation.||
26505|Crown Point Formation|71342|4|Described|Ch4 p25, Ch5 p5-p6|Early Permian|Late Carboniferous|Pedirka Basin. Formally defined by Wells et al (1966) to replace the informal Crown Point Series. A type section outcropping at One Tree Point on the FINKE 1:250000 map area in the NT is mentioned. Lithology discussed in further detail. This unit has a maximum thickness of 347m at Mount Hammersley 1. Sedimentology is briefly described. Deposited in periglacial, interglacial, fluvioglacial or glaciolacustrine environments. See also Ch5 p30, Ch5 p36, Ch5 p44-p48, Ch5 p51, Ch8 p28, Ch9 p9, Ch9 p11, Ch9 p16, Ch9 p18, Ch9 p20-p21, Ch11 p6-p7, Ch11 p18, Ch12 p7.||||Unconformably overlies the Finke Group. Disconformably overlain by the Purni Formation. Equivalent to the Boorthanna and Merrimelia Formations.|Pale grey to buff, very fine to coarse-grained sandstone with interbeds of medium to dark grey siltstone.|
26505|Crown Point Formation|72476|6|Mentioned|p26, p36 Fig.9|Permian|Carboniferous|Perdika Basin. Time-temperature thermal history diagram.||||||
26505|Crown Point Formation|73281|6|Mentioned|p1, Appendix (DIP)|||Pedirka Basin. See DIP034_Petroleumdata.xlsx.||||||
74010|Cultana Subsuite|65221|6|Mentioned|p26|||Brecciated unit. ?of Hiltaba Suite||||||
74010|Cultana Subsuite|65483|2|Defined|p17-26, Fig 2-4,7, Table 1|Calymmian|Calymmian|Felsic magmatic intrusion, of the Hiltaba Suite, 1584 +/-3 Ma Pb/Pb by ID-TIMS. Lithologies: quartz feldspar porphyry, alkali granite, feldspar-phyric monzogranite, alkali-feldspar microgranite and micro-syenogranite. Previously Cultana Granite etc.||||||04-MAR-13
74010|Cultana Subsuite|69666|5|Briefly described|p25, p28|Mesoproterozoic|Mesoproterozoic|Cultana Inlier.|c.1585 Ma.|Hiltaba Suite.||Is overlain unconformably by Beda Basalt.|Porphyritic.|
74010|Cultana Subsuite|70333|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|This unit has a map symbol labelled Mu1. It is not clear whether the units with symbols Mu2 to Mu5 (alkali-feldspar granite; feldspar-phyric granophyric monzogranite; alkali-feldspar microgranite; micro-syenogranite) are in the Cultana Subsuite or the parent Hiltaba Suite.||Probably of Hiltaba Suite.|||Quartz-feldspar porphyry, round quartz and small euhedral feldspar phenocrysts, pink-purple fine-grained granular groundmass of quartz, feldspar, minor haematite.|11-JAN-16
74010|Cultana Subsuite|70334|4|Described|p2,8,14-17,39-41,44,67-68,75-76,82,84-86|Statherian|Statherian|Geological province: Gawler Craton. Exposed in the Douglas Hills of the Cultana Inlier (McAvaney, 2009), and bound to the W by Cultana Fault. Has ID-TIMS age of 1584+\-3 Ma from quartz-feldspar porphyry sample. Comprises a range of comagmatic granitic and porphyritic lithologies with no cross-cutting relationships and transitional boundaries. Produced by fractionation of a more mafic magma (primitive-mantle normalised trace element patterns similar to other Hiltaba granites). Locally intruded by a haematised sandstone dyke of the Backy Point Formation. Unroofed during Cultana Inlier uplift.|1584+\-3 Ma (ID-TIMS)|Unit of Hiltaba Suite.||Overlain unconformably by Backy Point Formation or Beda Basalt. Intrudes into Moonabie Formation. Intruded by Gairdner Dolerite dykes.|Quartz-feldspar porphyry; alkali granite; feldspar-phyric granophyric monzogranite; alkali feldspar microgranite and syeno-microgranite.|
74010|Cultana Subsuite|71236|2|Defined|iii-v, p1, p3, p5-p7, p10-p13|Mesoproterozoic|Mesoproterozoic|Gawler Craton, Cultana Inlier. This unit is exposed in the Douglas Hills on the the north-eastern Eyre Peninsula and extends for up to 7km. This unit has been affected by iron-rich hydrothermal alteration. The name is derived from the Cultana Homestead, which is now located within the Cultana Army Training Area. The intrusive component of this unit has variously been referred to as the Cultana Granite, Cultana Granitic Complex, Cultana Granite Complex, Cultana Complex. It is redefined in this volume for numerous reasons (See p6). A type locality is assigned at Douglas Point and numerous reference localities are also assigned (see p6). Petrography and lithology of constituents discussed in detail. Pluton morphology, alteration, geophysical response and geochemistry discussed in detail. See also p15, p18-p20, p22, p24-p33.|1584 +/- 3 Ma (IDTIMS, Fanning 1990)|Hiltaba Suite||Intrudes the Moonabie Formation. Unconformably overlain by the Backy Point Formation. Intruded by the Gairdner Dolerite.|Feldspar porphyry, alkali granite, feldspar-phyric granophyric monzogranite, alkali feldspar microgranite and syeno-microgranite.|17-MAR-23
24236|Curdimurka Subgroup|22589|6|Mentioned|p129||Neoproterozoic|||||||
24236|Curdimurka Subgroup|22631|6|Mentioned|p177|Cryogenian|Cryogenian|||||||
24236|Curdimurka Subgroup|22772|4|Described|p65,Table13.1|Cryogenian|Cryogenian|||||||
24236|Curdimurka Subgroup|22857|5|Briefly described|Tb. 13.1 (insert p70-71)|Willouran|Willouran|Of the Callana Group.||||||
24236|Curdimurka Subgroup|22926|6|Mentioned|37|||Geol province Spalding Inlier. Parent Callana Group||||||
24236|Curdimurka Subgroup|23054|6|Mentioned|p11,34|||||||||
24236|Curdimurka Subgroup|24175|3|Fully described|p9|Neoproterozoic|Neoproterozoic|Of Callana Group.  Overlain by Burra Group.  Max. thickness: 4700m.||||||
24236|Curdimurka Subgroup|24321|5|Briefly described|Map legend|Adelaidean|Adelaidean|Parent: Callanna Group||||||
24236|Curdimurka Subgroup|24506|6|Mentioned|p17|Neoproterozoic|Neoproterozoic|||||||19-SEP-05
24236|Curdimurka Subgroup|24546|5|Briefly described|p2 - 3 Fig.2|Neoproterozoic|Neoproterozoic|Of Arkaroola Subgroup. Geological Province: Adelaide Fold Belt.||||||16-JAN-08
24236|Curdimurka Subgroup|24584|6|Mentioned|p14 Fig. 2|Neoproterozoic|Neoproterozoic|Marble.||||||
24236|Curdimurka Subgroup|24586|5|Briefly described|p51 Fig. 1|Adelaidean|Adelaidean|Upper part of Callanna Group (Warrina Supergroup).  Allochthonous breccia comprising sandstone, limestone and shale contained within a matrix of yellow-weathering dolomite and associated volcanics of the Callana Volcanics. Geol.Prov: Adelaide Geosyncline.||||||05-JUL-06
24236|Curdimurka Subgroup|37854|2|Defined|p9|Adelaidean|Adelaidean|See also p9.Willouran||||||12-MAR-14
24236|Curdimurka Subgroup|38004|6|Mentioned|p82|||||||||
24236|Curdimurka Subgroup|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Willouran to SturtianWillouran||||||
24236|Curdimurka Subgroup|39348|6|Mentioned|Map legend|Adelaidean|Adelaidean|Willouran||||||
24236|Curdimurka Subgroup|39490|6|Mentioned|p10|||||||||
24236|Curdimurka Subgroup|40225|6|Mentioned|Map sheet|||||||||
24236|Curdimurka Subgroup|40294|6|Mentioned|p8|||See also P12||||||
24236|Curdimurka Subgroup|41401|6|Mentioned|Table 4|||||||||
24236|Curdimurka Subgroup|41402|6|Mentioned|p42|||||||||
24236|Curdimurka Subgroup|41403|4|Described|p59|||||||||
24236|Curdimurka Subgroup|41404|6|Mentioned|p73|||||||||
24236|Curdimurka Subgroup|41405|6|Mentioned|p125|||||||||
24236|Curdimurka Subgroup|41526|6|Mentioned|p31|||||||||
24236|Curdimurka Subgroup|42098|6|Mentioned|Table 2 P54|||||||||
24236|Curdimurka Subgroup|42101|6|Mentioned|p84|||||||||
24236|Curdimurka Subgroup|42222|4|Described|p12|||||||||
24236|Curdimurka Subgroup|42223|5|Briefly described|p37|||||||||
24236|Curdimurka Subgroup|42238|5|Briefly described|p71|||||||||
24236|Curdimurka Subgroup|42720|5|Briefly described|map legend|Willouran||||||||
24236|Curdimurka Subgroup|42813|4|Described|p14|||of Callanna Group||||||
24236|Curdimurka Subgroup|43052|4|Described|p175|||of Callanna Group||||||
24236|Curdimurka Subgroup|43742|6|Mentioned|p37|||||||||
24236|Curdimurka Subgroup|43845|5|Briefly described|Fig2 p42, 44||Neoproterozoic|In Callanna Group||||||12-JUL-16
24236|Curdimurka Subgroup|44133|6|Mentioned|p52|||||||||
24236|Curdimurka Subgroup|44289|5|Briefly described|Map Legend||Neoproterozoic|||||||
24236|Curdimurka Subgroup|60718|5|Briefly described|p49 Fig. 2, p50|Adelaidean|Adelaidean|Geol Prov: Adelaide Geosyncline. See also p51 Fig. 3.||Of Callanna Group.|Includes: Boorloo Siltstone, Coranna Fm, Hogan Dolomite; Recovery Fm, Dunns Mine Limestone, and Rook Tuff; and Dome Sandstone, from top to bottom.|||15-APR-11
24236|Curdimurka Subgroup|60959|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Of the Callanna Group.||||||
24236|Curdimurka Subgroup|62592|5|Briefly described|p20 Fig.2.4, p50 Table 5.1, p57.|Willouran|Willouran|Deposited in deeply subsiding graben structures during rifting. Colour scheme shown for interpretation of Curnamona seismic sections. Written as SubGroup.||Unit in Callanna Group.|||Clastics, carbonates, evaporites.|
24236|Curdimurka Subgroup|62664|5|Briefly described|p138 Fig.2.|Neoproterozoic|Neoproterozoic|||Unit in upper Callanna Group.|Includes Rook Tuff.|Unconformably overlies Arkaroola Subgroup. Is unconformably overlain by Burra Group.|Sandstone, siltstone, shale, carbonates, tuff.|
24236|Curdimurka Subgroup|62724|6|Mentioned|p16, p21|||Evaporitic clastic and carbonate sediments. Mostly absent from Curnamona Province - particularly over Olary Domain where it is eroded away.||||||07-FEB-11
24236|Curdimurka Subgroup|64793|6|Mentioned|p284 fig 3, p285|||||Unit in Callanna Group.|Includes Rook Tuff.|||
24236|Curdimurka Subgroup|64796|6|Mentioned|p183 fig 2, p184, p187-188, p200-202|Neoproterozoic|Neoproterozoic|Of Adelaide Rift Complex. Type area in Willouran Ranges.||Unit in Callanna Group.|Includes Rook Tuff.|||
24236|Curdimurka Subgroup|64797|5|Briefly described|p151, p158, p163, p164 Fig.11 |||See also p169 Fig.12 . S-isotope data. International correlations.|800 Ma.|Unit in Callanna Group.|Includes River Broughton beds.|||
24236|Curdimurka Subgroup|65365|5|Briefly described|p10 Fig. 4|Cryogenian|Cryogenian|Adelaide Rift Complex / Stuart Shelf. Includes Rook Tuff dated at 802 +/- 10 Ma, U-Pb (Fanning, 1986).||||||19-MAR-12
24236|Curdimurka Subgroup|65366|5|Briefly described|p23 Fig. 3|Cryogenian|Cryogenian|Adelaide Rift Complex / Stuart Shelf. Includes Rook Tuff dated at 802 +/- 10 Ma, U-Pb (Fanning, 1986).||||||19-MAR-12
24236|Curdimurka Subgroup|65379|5|Briefly described|p643, p644, p646|Neoproterozoic|Neoproterozoic|Of Callanna Group (Warrina Supergroup). Siltstone, dark-grey; sandstone; dolomite; limestone, stromatolitic. N.B.  Asbestos deposit host, contains Adams, Arkaba, Peate and Mt Lyndhurst asbestos prospects, and Oraparinna asbestos mine.||||||07-MAR-12
24236|Curdimurka Subgroup|66522|5|Briefly described|p19.|Neoproterozoic|Neoproterozoic||||Includes Rook Tuff.|||
24236|Curdimurka Subgroup|66884|6|Mentioned|p36, p41 Fig.3|||Age: Willouran||Callanna Group|||Megabreccia.|
24236|Curdimurka Subgroup|67870|5|Briefly described|p9|Neoproterozoic|Neoproterozoic|Adelaide Rift System.||Callanna Group.|Rook Formation.|||
24236|Curdimurka Subgroup|67979|5|Briefly described|p528|Cryogenian|Cryogenian|||of the upper Callanna Group|includes Rook Tuff|||
24236|Curdimurka Subgroup|69019|4|Described|p36-38, p66.|Neoproterozoic|Neoproterozoic|Cyclic sequences of clastics and carbonates deposited under partly evaporitic conditions, partly in fault controlled basins. Age from Rook Tuff in adjacent map area.|802 +/- 10 Ma (U-Pb zircon: Fanning et al. 1986).|Unit in Callanna Group.|Includes Recovery Formation, Cooranna Formation, Boorloo Siltstone.||Siltstone: laminated, carbonaceous, lithic, pyritic and micaceous; sandstone: feldspathic to lithic, cross-bedded and ripple-marked; stromatolitic dolomite and limestone.|
24236|Curdimurka Subgroup|69666|6|Mentioned|p33||||||Rook Tuff.|||
24236|Curdimurka Subgroup|69873|6|Mentioned|p82|||Adelaide Rift Complex. Included in diagram showing Cryogenian-Ediacaran stratigraphy and correlations with Tasmanian succession.|||Includes Rook Tuff.|||
24236|Curdimurka Subgroup|70334|5|Briefly described|p38|||Geological province: Gawler Craton. Of Adelaide Geosyncline.||Unit of Callana Group.||||
24236|Curdimurka Subgroup|70405|6|Mentioned|p97|Neoproterozoic|Neoproterozoic||||||Clastic-carbonate-evaporite sediments.|
24236|Curdimurka Subgroup|70407|5|Briefly described|p102 Fig 1, p103 Fig 2|Neoproterozoic|Neoproterozoic|Age: Willouran||Of Callanna Group.||||
24236|Curdimurka Subgroup|70819|6|Mentioned|p13|Neoproterozoic|Neoproterozoic|Clare Valley.||Callanna Group.|Rook Tuff.|||
24236|Curdimurka Subgroup|72456|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Marree 1:250k map sheet. |||||Siltstone, dark grey, carbonaceous, lithic, pyritic, laminated, micaecous; sandstone, feldspathic, lithic, cross-bedded, halite clasts; dolomite, stromatolitic, cryptalgal laminated, brown to yellow weathering; limestone, stromatolitic.|
24236|Curdimurka Subgroup|72492|3|Fully described|p1, p2-3, p5 Fig.4, p5 Fig.5|Neoproterozoic|Neoproterozoic|Type locality said to be in Willouran Ranges. Interpreted as a coastal sabkha or playa lake environment that became progressively more restricted from south to north. Alternative interpretation is alkaline lake environment, like East African rift valley, but this paper dismisses this option. See also p17-18. Samples collected from the type locality in the Willouran Ranges. Misspelt as Curdimurka Subroup twice on p2.|802 +/- 10 Ma|Callanna Group|Dome Sandstone, Rook Tuff, Dunns Mine, Waraco Limestones, Recovery, Cooranna Formations, Hogan, Worumba Dolomites, Boorloo Siltstone, Wirrawilka, Niggly Gap, Arkaba Hill beds, Kirwan Siltstone.|Overlies Arkaroola Subgroup.|Includes cyclically alternating siliciclastic sediments, carbonates, evaporites and minor volcanic flows. Major outcrop areas occur in the Peake and Denison Ranges, the Willourian Ranges, the Worumba Anticline and the Spalding Inlier.|16-SEP-20
24236|Curdimurka Subgroup|73093|5|Briefly described|map legend|Neoproterozoic|Neoproterozoic||||||Carbonaceous-pyritic siltstone and feldspathic-lithic sandstone, stromatolitic limestone and dolomite, minor felsic volcanics and volcaniclastics.|09-DEC-21
24236|Curdimurka Subgroup|73222|5|Briefly described|p6-7, p21|Tonian|Tonian|Adelaide Rift Complex. Upper part of the Callanna Group. Outcrops in the Willouran Ranges.||Callanna Group, Warrina Supergroup|Dunns Mine and Waraco limestones, Dome Sandstone; Boorloo and Kirwan siltstones; Hogan and Worumba dolomites; Cooranna and Recovery formations; Rook Tuff; Arkaba Hill, Niggly Gap, and Wirrawilka Beds|Underlain by Arkaroola Subgroup.||
24236|Curdimurka Subgroup|74367|5|Briefly described|p7 Fig.6, p8, p18, p20|Tonian|Tonian|Suggested to include the Oodla Wirra Volcanics based on evaporite mineralogy and SHRIMP ages. Age of 802+/-10 Ma from Rook Tuff (Fanning et al., 1986). Not deposited in the Arkaroola area.|802+/-10 Ma|Callanna Group|Dome Sandstone, Rook Tuff, Niggly Gap Beds, Recovery Formation, Cooranna Formation, Boorloo Siltstone|||
35326|Curnamona Group|23345|5|Briefly described|43|||||||||
35326|Curnamona Group|23346|6|Mentioned|48|||||||||
35326|Curnamona Group|23347|2|Defined|p51 Tb. 1, p52, p53 Fig. 3|Statherian|Statherian|Lower part of Willyama Supergroup. Age: 1.712+/-2Ma. Dominates southern portion of Olary Domain. Metasediment-dominated, volcano-sedimentary sequence. Incorporates Bimba, calcsilicate, quartzofeldspathic and composite gneiss suites of Clarke et al (1986)||||||30-APR-13
35326|Curnamona Group|23476|5|Briefly described|p50 Fig 1|||||||||
35326|Curnamona Group|24289|5|Briefly described|p46, p47 Fig.2|Paleoproterozoic|Paleoproterozoic|Geological Province: Curnamona Province.||||||07-NOV-08
35326|Curnamona Group|24431|5|Briefly described|p189 Fig. 1|||Overlain by the Strathearn Group. Geological Province: Olary Domain.||||||
35326|Curnamona Group|60485|5|Briefly described|p28 Fig. 2|||Of the Willyama Supergroup.  Includes the Ethiudna and Wiperaminga Subgroups, and the Bimba Formation. Geological Province: Olary Domain.||||||03-MAR-05
35326|Curnamona Group|61734|5|Briefly described|p52 Fig.2, p54-57, p68 Fig.9, p71|Statherian|Statherian|||Of the Willyama Supergroup.|Includes the Bimba Formation, Ethiudna and Wiperaminga Subgroups.|Underlies the Strathearn Group. Is intruded by Basso and Lady Louise Suites.|Migmatite dominated. Comprises variably oxidized, magnetite-bearing quartzofeldpathic gneiss, calc-silicate and calc-albitite gneiss and psammopelitic schist.|21-JUL-20
35326|Curnamona Group|61736|4|Described|p666 Fig. 3, p670|Paleoproterozoic|Paleoproterozoic|Subdivided into Wiperaminga and Ethiudna Subgroups. Overlain by Strathearn Group. Geological province: Olary Domain.||||||24-FEB-10
35326|Curnamona Group|62373|5|Briefly described|p503 Fig.2|Paleoproterozoic|Paleoproterozoic|Comprises Ethiudna and Wiperaminga Subgroups. Geological Province: Curnamona Province/Olary Domain.||||||07-NOV-08
35326|Curnamona Group|62514|5|Briefly described|p748 Fig. 3|Mesoproterozoic|Mesoproterozoic|Includes Wiperaminga and Ethiudna Subgroups, and Bimba Formation.  Age: <1700Ma. Geological Province: Olary Domain/Curnamona Province||||||16-SEP-09
35326|Curnamona Group|62535|4|Described|p666, p670, p672-674|Paleoproterozoic|Paleoproterozoic|Olary Domain. Hosts various types of oxide-, sulfide-, and silicate-facies iron formation with minor strata-bound Cu, Co and/or Au deposits.|~1715 Ma.||Wiperaminga, Ethiudna Subgroups.|Is overlain by Strathearn Group. Interbedded with Basso Suite.|Oxidised package of metasedimentary and metavolcanic rocks.|
35326|Curnamona Group|62592|5|Briefly described|p14, p15, p16 Fig.2.2, p43.|||Olary Domain. Deposition within an extensional environment. Shown as including Bimba Formation in Fig.2.2.||Basal unit in Willyama Supergroup.|Includes Wiperaminga and Ethiudna Subgroups.|Is intruded by Basso Suite and Lady Louise Suite. Is overlain unconformably by Strathearn Group.|Quartzofeldspathic, locally calcareous and evaporitic in upper parts.|
35326|Curnamona Group|62724|5|Briefly described|p20 Fig. 10|Paleoproterozoic|Paleoproterozoic|Of the Willyama Supergroup.  Geological Province: Curnamona Province.||||||07-FEB-11
35326|Curnamona Group|62993|5|Briefly described|p1, 3, 12, 14, 15, 35, 37, 39, 40, 44|Paleoproterozoic|Paleoproterozoic|Olary Domain. Oldest part of Willyama Supergroup.|~1720-1750 Ma|Willyama Supergroup|Includes Ethiudna Subgroup, Wiperaminga Subgroup|Intruded by Basso Suite||19-DEC-21
35326|Curnamona Group|63020|5|Briefly described|p987 Fig. 8|Paleoproterozoic|Paleoproterozoic|Geological Province: Curnamona Province (Olary Domain).||||||07-NOV-08
35326|Curnamona Group|63102|4|Described|p9-10,13-15,19-20,26,32-33,35,37-38|Statherian|Statherian|Geological province: Olary Domain, Curnamona Province. Also known as lower Willyama Supergroup, in the Olary Domain. Deposition of syngenetic and/or diagenetic sulphides, iron formations, barite, Mn-rich rocks. Diagenetic sodic alteration. Of low grade metamorphic facies; albite+\-K-feldspar, quartz, biotite and calcite in feldspathic (and calc-feldspathic) compositions; also contains sillimanite and andalusite (sericite pseudomorphs). Characterised by hot A-type volcanism (~1710 Ma). Coeval with Basso Suite emplacement. Overprinted by oxidesed albite-magnetite alternation; tends to show higher degree of metamorphic alteration and partial meting (but not necessarily metamorphic grade) than higher parts of the Willyama Supergroup. Cu-Au mineralisation preferentially concentrated in the lower part of Willyama Supergroup, near the top of Curnamona Group.  See also p44,51-54,72/||Unit of Willyama Supergroup.|Includes Bimba Formation, Ethiudna and Wiperaminga subgroups.||A-type volcanic rocks.|22-OCT-19
35326|Curnamona Group|63186|5|Briefly described|p67 Fig. 3, p70, p71 Fig. 5|Paleoproterozoic|Paleoproterozoic|Of the Curnamona Group (Willyama Supergroup). Age: 1607+/-17 Ma; also 1705 Ma. Geological Province: Olary Domain, Curnamona Province.||||||25-MAR-09
35326|Curnamona Group|63539|5|Briefly described|p33|||Has contact with Strathearn Group. Geological Province: Olary Domain.||||||07-FEB-08
35326|Curnamona Group|63866|4|Described|p40-p42|||Olary Domain, Curnamona Province. Hosts Cu-Au (-Mo) mineralisation as stratabound replacement and vein networks.|1719 Ma|Willyama Supergroup|Includes the Wiperaminga and Ethiudna Subgroups.|Intruded by the Basso Suite.||
35326|Curnamona Group|64097|5|Briefly described|p306|||Age: 1720-1710Ma. Geological province: Olary Domain.||||||07-FEB-11
35326|Curnamona Group|64741|5|Briefly described|p300, p301 Fig. 4|Paleoproterozoic|Paleoproterozoic|Of Willyama Supergroup. Includes Wiperaminga and Ethiudna Subgroups. Includes Wiperaminga and Ethiudna Subgroups. Geological province: Olary Domain, Curnamona province. Predominantly metasedimentary.||||||07-FEB-11
35326|Curnamona Group|64742|5|Briefly described|p320,  pp325-326, p330.|||Olary Domain. Variably albitised volcano-sedimentary sequence. Major and trace element analyses, and Sm-Nd isotope data, are detailed.||Unit in Willyama Supergroup.|Includes Wiperaminga and Ethiudna Subgroups, and Basso Suite.|Is overlain by Strathearn Group.||29-MAR-12
35326|Curnamona Group|64944|5|Briefly described|p27, p28 Fig. 1, p29 Tb. 1|Paleoproterozoic|Paleoproterozoic|Of the Willyama Supergroup. Subdivided into the lower Wiperaminga and upper Ethiudna Subgroups and associated with the Basso Suite. Age: 1719-1708Ma.||||||07-FEB-11
35326|Curnamona Group|65407|5|Briefly described|p239 Fig.3|||Hosts stratiform to stratabound Zn-Pb-Ag.|||Ethiudna, Wiperaminga Subgroups.||Interbedded calc-silicate and albitic siltstone.|
35326|Curnamona Group|66302|6|Mentioned|p8, p35-37, p39, p76 fig 20|||Olary Domain, Curnamona Province.||Willyama Supergroup|Includes the Wiperaminga Subgroup and the Ethilduna Subgroup|||
35326|Curnamona Group|67323|5|Briefly described|Eastern Australia Time-Space Plot; p33|||Olary Domain, Curnamona Province. Deposited during intra-continental extension.|~1720-1690 Ma.||Ethiudna, Wiperaminga Subgroups.|Is intruded by Basso Suite and Poodla Hill Granite.||
35326|Curnamona Group|67536|5|Briefly described|Map Legend|Statherian|Statherian|Curnamona Province.|ca. 1710 Ma|Of the Willyama Supergroup.|||Schistose, albitic and calcsilicate metasediments.|
35326|Curnamona Group|67540|6|Mentioned|p29 Tb.2|||||||||04-FEB-16
35326|Curnamona Group|67653|5|Briefly described|p4-5,11|||Geological province: Curnamona Province. ||Unit of Willyama Supergroup.||||
35326|Curnamona Group|68067|6|Mentioned|Map legend.|||Areas with higher magnetic response are mapped separately.||||||27-AUG-13
35326|Curnamona Group|68126|4|Described|p6, p8, p15, p26, p29-30|Paleoproterozoic|Paleoproterozoic|Olary Domain. Represents the oldest metasediments in the Curnamona Province.|c.1720-1715 Ma (Conor and Preiss, 2008).|Willyama Supergroup.|Ethiudna, Wiperaminga Subgroups; Bimba Formation.||Schistose, albitic and calc-silicate metasediments.|
35326|Curnamona Group|69213|5|Briefly described|p32, 34, 24|Paleoproterozoic|Paleoproterozoic|Olary Domain, Curnamona Province. Includes migmatites of Olarian [Orogeny] age.|~1600 Ma|Willyama Supergroup.|Includes Wiperaminga Subgroup, Ethiudna Subgroup||Migmatites.|18-JAN-17
35326|Curnamona Group|69650|6|Mentioned|p6, p36|||||||||
35326|Curnamona Group|69999|5|Briefly described|p3|Paleoproterozoic|Paleoproterozoic|Curnamona Province. Basal, early-rift fluviatile to shallow marine sedimentation.||||||
35326|Curnamona Group|70000|5|Briefly described|p31, p33-35|Statherian|Statherian|Oldest rocks of the Curnamona Province. Deposited as shallow marine shelf sediments in a restricted saline, oxidised basin. Protolith was relatively sandy shallow marine sedimentary rocks with a possible evaporitic or hypersaline component represented by albitic horizons. Minor Fe oxide/sulfide +/- Cu mineralisation occurs in upper parts, associated with probable exhalative horizons (eg Iron Blow).|c.1720-1710 Ma.|Unit in Willyama Supergroup.|||Includes variably magnetite-rich, micaceous, siliceous and albitic metasedimentary rocks.|
35326|Curnamona Group|70015|5|Briefly described|Map legend|Statherian|Statherian|The three facies are mapped separately. Mineral deposits (if any) are shown.|c.1720-1710 Ma.|Unit in Willyama Supergroup.|||Micaceous, siliceous and albitic metasedimentary rocks; with moderate magnetite; magnetite-rich.|
35326|Curnamona Group|70339|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|||Willyama Supergroup.|||Metasediments characterised by calc-silicate minerals and alkali feldspar, magnetite or haemetite-bearing; local iron formation, some barite-bearing. Includes volcanogenic metasediments related to Abminga Subsuite.|02-FEB-16
35326|Curnamona Group|70340|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic||||||Metasediments characterised by calc-silicate minerals and alkali feldspar, magnetite or haemetite-bearing; local iron formation, some barite bearing. Includes volcanogenic metasediments related to Abminga Subsuite.|
35326|Curnamona Group|70405|4|Described|p9 table 1,p1,p15, p38, p43 Table 3,p95|Paleoproterozoic|Paleoproterozoic|Metasediments are dominated by quartz and feldspar. Shale siltstone and clay rich sandstone are the likely protoliths of this group and its subgroups.Correlated with Thackaringa Group previously (now known to be incorrect).|1710 Ma-1720 Ma|Wilyama Supergroup|Includes Wiperaminga Subgroup, Ethiunda Subgroup,|Intruded by Basso Suite,disconformably underlies Bimba Formation|Albitic metasediments with psammitic, psammopelitic, pelitic, calcsilicate and calc-albitite metasediments. Interbedded with quartzite and bimodal (dominantly felsic) volcanics - porphyritic rhyolite, metatuffs and volcaniclastic metasediments.|
35326|Curnamona Group|70657|4|Described|p5-7, p10, p11 Fig.5, p12, p13 Fig.6|Statherian|Statherian|See also p14-17, p21, p24-25, p33, p36-37, p41, p43, p45-46, p51, p57-59. Curnamona Province, Olary Domain. The Bimba Formation has been moved into the Saltbush Group on geochronology grounds. The Portia Formation is not part of the Curnamona Group. Coeval magmatism includes both felsic and mafic components. The Curnamona Group of the Olary Domain is characterised by the Basso Suite. Quartz-magnetite and barite-rich units are present throughout. Deformation discussed in detail. Intense oxidised Na-(K)-Fe alteration described.|~1720 - ~1710 Ma|Lower Willyama Supergroup|Includes Wiperaminga Subgroup, Ethiudna Subgroup.|Underlies Bimba Formation (Larry Macs Subgroup, Saltbush Group), Portia Formation. Interlayered with extrusive flows of Basso Suite. Is intruded by Lady Louise Suite.|Includes dominantly A-type felsic volcanics with later basaltic magmatism.|
35326|Curnamona Group|70658|5|Briefly described|p1-2, 5-6, 15, 47|Paleoproterozoic|Paleoproterozoic|Olary Domain, Curnamona Province. Rapid deposition in shallow water.||Willyama Supergroup.|Ethiudna, Wiperaminga Subgroups.|Associated with the Basso Suite.||
35326|Curnamona Group|71968|6|Mentioned|p4|||Geological province: Curnamona province.||||||
35326|Curnamona Group|72454|6|Mentioned|p2 Fig.2, p8 Fig.6|Mesoproterozoic|Mesoproterozoic|Part of the Olary Domain.||Willyama Supergroup|Includes Bimba Formation.|||
35326|Curnamona Group|73429|5|Briefly described|p106 Fig.2, p107-108, p110, p111 Fig.6|Statherian|Statherian|Curnamona Province, Olary Domain. Location in text includes p112 Fig.7.||Willyama Supergroup, lower|Wiperaminga Subgroup, Ethiudna Subgroup.|Unconformably underlies Saltbush Group|Includes magnetic psammopelites.|
35326|Curnamona Group|73512|6|Mentioned|p2|||||||||
39162|Curramulka Gabbronorite|24475|2|Defined|p56|Mesoproterozoic|Mesoproterozoic|Intrudes Aagot Member of the Wandearah Formation. Intruded by Hiltaba Suite. Overlain by Winulta Formation.||||||
39162|Curramulka Gabbronorite|24585|5|Briefly described|p32|Calymmian|Calymmian|Intrudes the Wallaroo Group. Age: ~1589Ma.||||||23-DEC-09
39162|Curramulka Gabbronorite|60958|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Medium to coarse grained gabbronorite with plagioclase, clinopyroxene (augite), orthopyroxene, hornblende, biotite quartz or orthoclase. Intrudes Aagot Member and intruded by Arthurton Granite. Age: 1589 +/- 5Ma. Geological Province: Gawler Craton.||||||21-FEB-14
39162|Curramulka Gabbronorite|61121|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Medium- to coarse-graine dgabbronorite with plagioclase, clinopyroxene (augite) orthopyroxene, hornblende, biotite, quartz or orthoclase. Intrudes Aagot Member;  intruded by Arthurton Granite. Age: 1589+/-5Ma. Geological Province: Gawler Craton.||||||02-JUN-05
39162|Curramulka Gabbronorite|62963|5|Briefly described|p28, p29|Mesoproterozoic|Mesoproterozoic|Age: 1583+/-6.6Ma.  Geological province: Gawler Craton, Yorke Peninsula region.||||||
39162|Curramulka Gabbronorite|63398|5|Briefly described|p662, p663|Mesoproterozoic|Mesoproterozoic|Subsurface  plutonic body; surrounded/intruded by Arthurton Granite. Intruded the Wallaroo Group. Age: 1588+/-15Ma (zircon). Geological Province: Gawler Craton. See also p671 Fig. 7.||||||10-DEC-07
39162|Curramulka Gabbronorite|65375|4|Described|p13, p20, p23, p48.|Mesoproterozoic|Mesoproterozoic|Subsurface mafic intrusion into metasandstone and metaconglomerate in the Curramulka area, equivalent to Aagot Member. Has a close relationship with Arthurton Granite. c.10 x 20 km in size. Composition is variable, suggesting a high degree of crustal assimilation.|1588.6 +/- 4.8 Ma.|||Intrudes Wallaroo Group.|Consists mainly of plagioclase, augite, orthopyroxene, hornblende, biotite, +/- quartz or orthoclase.|
39162|Curramulka Gabbronorite|65376|6|Mentioned|p101 Fig.3.1.||||1583 Ma.|||||
39162|Curramulka Gabbronorite|65390|6|Mentioned|p23 Fig.3|Calymmian|Calymmian|Olympic Domain, Gawler Craton. Age of about 1590 Ma inferred in Figure 3.||||||
39162|Curramulka Gabbronorite|66302|6|Mentioned|p47|Calymmian|Calymmian|Igneous crystallisation age. |1589 +/- 5 Ma (Zang et al, 2002)|Hiltaba Suite|||Continental tholeiitic gabbronorite.|
39162|Curramulka Gabbronorite|67536|6|Mentioned|Map Legend|Calymmian|Calymmian|Gawler Craton. Age constrained by the parent Hiltaba Suite.|ca. 1583 +/- 5 Ma|Of the Hiltaba Suite.||||
39162|Curramulka Gabbronorite|67900|6|Mentioned|p22, 32|Mesoproterozoic|Mesoproterozoic|Yorke Peninsula, Gawler Craton.|1589 +/- 5 Ma.|||||
39162|Curramulka Gabbronorite|69748|6|Mentioned|p180|||Moonta-Wallaroo region, Olympic IOGC Province.|1583 +/- 3 Ma (Zang et al., 2007).|Hiltaba Suite.||||
39162|Curramulka Gabbronorite|70334|5|Briefly described|p75|Calymmian|Calymmian|Geological province: Gawler Craton. Early phase of mafic magmatism during lithospheric extension, asthenospheric mantle upwelling, partial mantle melting and associated higher mantle heat flow contemporaneous with the early phase of Gawler Range volcanism.||||||
39162|Curramulka Gabbronorite|72725|6|Mentioned|p41, p43-44|Calymmian|Calymmian||1583 +/- 5 Ma|||||
39162|Curramulka Gabbronorite|72949|6|Mentioned|p36|Calymmian|Calymmian|Olympic Domain, south. Yorke Peninsula / Eastern Eyre Peninsula.|1589 +/- 5 Ma|||||
39162|Curramulka Gabbronorite|73026|5|Briefly described|p9-10|Mesoproterozoic|Mesoproterozoic|Appears as Curamulka Gabbronorite.|1583 +/- 5 Ma||||Gabbronorite plug.|
39162|Curramulka Gabbronorite|73027|5|Briefly described|p9,|Mesoproterozoic|Mesoproterozoic||1583 +/- 5 Ma|||||
39162|Curramulka Gabbronorite|73092|6|Mentioned|p2|Mesoproterozoic|Mesoproterozoic|||||||
39162|Curramulka Gabbronorite|73165|6|Mentioned|p620 Fig. 1, 622|||Gawler Craton. Moonta Domain, northern Yorke Peninsula. Mafic component of Hiltaba Suite.||Hiltaba Suite||||
39162|Curramulka Gabbronorite|73493|5|Briefly described|p725 Fig.12|Calymmian|Calymmian||ca 1595 Ma (Wade et al., 2019)|Hiltaba Suite||||
39162|Curramulka Gabbronorite|73644|5|Briefly described|p3|Mesoproterozoic|Mesoproterozoic|||Hiltaba Suite||||
25688|Dalhousie Formation|40925|6|Mentioned|Map legend|Cenozoic|Cenozoic|||||||19-NOV-08
25688|Dalhousie Formation|40926|3|Fully described|p36|||||||||
25688|Dalhousie Formation|41098|6|Mentioned|p179|||||||||
25688|Dalhousie Formation|42905|5|Briefly described|p24, Fig 5.3|||||||||
82254|Daly Head Metadolerite|73493|3|Fully described|p711-713, p717-718, p723-728, p732|Calymmian|Calymmian|Gawler Craton, Yorke Peninsula. Outcrop limited to coastal zones. Previously correlated with Tournefort Metadolerite in regional mapping, and referred to as Tournefort Metadolerite (Zang, 2006) and 'Type 2 mafic dykes' Reid et al. (2008). Defined as new unit in this study. Name derived from Daly Head on KINGSCOTE 1:250 000 sheet. Distribution of northern KINGSCOTE and southwestern MAITLAND 1:250 000 sheets. Type locality of Royston Head, reference locality of Daly Head. Geochemical correlation made with other straight-sided dykes in region. Cross-cut deformation fabrics within Donington Suite. Some examples are cross-cut by narrow high-strain zones, within which is a syn-kinematic granite dated to ca 1555 Ma. See also p715 Fig.2, p716 Fig.3, p721 Fig.8, p722 Fig.9.|1563+/-4 Ma SHRIMP U-Pb zircon at Royston Head|Nil|Royston Head mafic dykes, Southern Yorke Peninsula mafic dykes|Intrudes Donington Suite|Metadolerite composed of hornblende-plagioclase-biotite+/-clinopyroxene+/-quartz. Dykes are 0.5-8 m wide, may have chilled margins and a weak alignment of hornblende and biotite, clinopyroxene typically partly regressed to amphibole. Tholeiitic.|
23531|Danae Conglomerate Member|24175|5|Briefly described|p40|Tertiary|Tertiary|Of the Mirikata Formation.  Underlies Millers Creek Dolomite Member.  Geological Province: Billa Kalina Basin.||||||
23531|Danae Conglomerate Member|36966|3|Fully described|p89|||||||||
23531|Danae Conglomerate Member|38108|6|Mentioned|Table 1|||||||||
23531|Danae Conglomerate Member|38605|6|Mentioned|Table 5|||||||||
23531|Danae Conglomerate Member|42375|6|Mentioned|p79|||Member of Mirikata Formation.||||||
23531|Danae Conglomerate Member|42465|5|Briefly described|Map Legend|||||||||
23531|Danae Conglomerate Member|42469|4|Described|p40|||||||||
23531|Danae Conglomerate Member|42723|5|Briefly described|map legend|Miocene||||||||
23531|Danae Conglomerate Member|43048|4|Described|Table 3.|||||||||
23531|Danae Conglomerate Member|44133|5|Briefly described|p190 Fig. 10.30|Miocene|Miocene|Geological Province: Billa Kalina Basin. Of the Mirikata Formation. Thickness: 3m. Gradationally underlies: Billa Kalina Clay Member.||||||
23531|Danae Conglomerate Member|64696|5|Briefly described|p133 Figs.13,14 |Miocene|Miocene|||Of the Mirikata Formation.||||
23531|Danae Conglomerate Member|67462|5|Briefly described|Map legend.|Miocene|Miocene|Billa Kalina Basin.||Unit in Mirikata Formation.||||
23531|Danae Conglomerate Member|68715|6|Mentioned|p30 Fig.5|Langhian|Burdigalian|Billa Kalina Basin.||||||
83519|Danae Hill Metavolcanics|73155|5|Briefly described|p277, p282 Fig.13, p283, p285 Tb.1|Archean|Archean|Gawler Craton. Possible equivalent to Devil's Playground Volcanics. Variable magnetic character. Uncertainty indicated for Archean age p285 Tb.1.Spelt Danae Hills Metavolcanics p285.|||||Dominantly basaltic volcanics.|05-SEP-22
75848|Darke Peak Group|66882|3|Fully described|p99; p103-104 Figs.3c,4; p113-121|Orosirian|Orosirian|New name. West of Kalinjala Mylonite Zone. Replaces part of (superseded) Hutchison Group.  Lincoln-Cleve Uplands. Grouping is based on combining U-Pb, Sm-Nd isotopic and geochemical data. Metasediments sourced from Gawler Craton. Also repeatedly mis-spelt as Dark Peak on p121.|c.1865 Ma.||Includes Bosanquet Formation, Yabmana Iron Formation, Poolalalie Dolomite and Warrow Quartzite.|Disconformably underlies Cleve Group.|A-type felsic volcanics (rhyolite), quartzite, pelite and carbonate rocks.|
75848|Darke Peak Group|67900|6|Mentioned|p20|Paleoproterozoic|Paleoproterozoic|Szpunar et al. (2011). Eastern Gawler Craton. Formerly part of the Hutchison Group. Appears as Darke Peake Group.|c.1860 Ma.|||||
75848|Darke Peak Group|70027|6|Mentioned|p56-57|Orosirian|Orosirian|Geological province: Gawler Craton. Deposited ca. 1865 Ma.|ca. 1865 Ma|||||
75848|Darke Peak Group|73026|5|Briefly described|p6-7, p14, p25, p29|Paleoproterozoic|Paleoproterozoic|Central/western Eyre Peninsula. Seperated out from the Hutchison Group by Szpunar et al(2011) on the basis of zircon studies. Has age components at c. 2520-2440 Ma and c. 2000Ma.|c. 1860 Ma|||||
75848|Darke Peak Group|73027|5|Briefly described|p7, p9, p14|Orosirian|Orosirian|Rocks belonging to this group previously belonged to the Hutchison Group.|c. 1860 Ma -1750 Ma|Hutchison Supergroup|||Quartzite and calc-silicate.|
75848|Darke Peak Group|73155|6|Mentioned|p279|Orosian|Orosian|Gawler Craton. Interpreted to have been deposited synchronously with volcanic rocks at ca. 1865 Ma (Szpunar et al., 2011).|ca. 1865 Ma|Hutchison Group, middle part|||Metasedimentary rocks.|
75848|Darke Peak Group|73234|6|Mentioned|p19|Orosirian|Orosirian|Eyre Peninsula, north-eastern. Age range from Szpunar et al. (2011).|Between c. 2000 Ma and c. 1865 Ma|||||
75848|Darke Peak Group|73235|6|Mentioned|p53, p58|Orosirian|Orosirian|Gawler Craton. Cleve, Coulta, Gawler Range Volcanic regions. Hosts Waddikee orogenic gold mineralisation and Moonlight intrusion-related gold mineralisation in the Waddikee mineral field of the Kimban gold mineral system. [Also indicate to host Weednanna and Bartels orogenic gold mineralisation; see Fig. 2].|c. 2000-1865 Ma||||[May include graphitic schist, amphibolite, and marble].|
75848|Darke Peak Group|73516|5|Briefly described|p11|Paleoproterozoic|Paleoproterozoic||||||Metasediments. Amphibolite to granulite grade metamorphism.|
75848|Darke Peak Group|73525|5|Briefly described|p19 Fig.13|||Cleve Domain.|||Warrow Quartzite, Poolalie Dolomite, Yabmana Iron Formation, Bosanquet Formation||Siliciclastics, carbonates, felsic extrusives.|
72576|Dayana Formation|61736|5|Briefly described|p666 Fig. 3|Paleoproterozoic|Paleoproterozoic|Of Mount Howden Subgroup (Strathearn Group). Geological province: Olary Domain.||||||
72576|Dayana Formation|62535|5|Briefly described|p666 Fig.3, p672|Paleoproterozoic|Paleoproterozoic|Olary Domain.||Mount Howden Subgroup.||||
72576|Dayana Formation|62993|6|Mentioned|p37|Paleoproterozoic|Paleoproterozoic|Olary Domain.||Mount Howden Subgroup||Overlies Mooleulooloo Formation||15-DEC-21
72576|Dayana Formation|64741|5|Briefly described|p301 Fig. 4, p311|Paleoproterozoic|Paleoproterozoic|Of Strathearn Group. Geological province: Olary Domain. Possible equivalent of Dalnit Bore Metasediments.||||||07-FEB-11
72576|Dayana Formation|64742|6|Mentioned|p321 Fig.3, P323. |||||Unit in Mount Howden Subgroup.|||Pelitic schist.|
72576|Dayana Formation|64944|4|Described|p28 Fig. 1, p29 Tb. 1|Paleoproterozoic|Paleoproterozoic|Of Strathearn Group. Geological province: Olary Domain. Fine-grained sillimanite-andalusite-staurolite schist. Equivalent to Dalnit Bore in Broken Hill Domain.||||||07-FEB-11
72576|Dayana Formation|66302|4|Described|p36 Fig.9, p38, p39|Statherian|Statherian|Olary Domain, Curnamona Province.||Mount Howden Subgroup||Overlies the Mooleulooloo Formation.|Fine-grained sillimanite-andalusite-staurolite schist.|
72576|Dayana Formation|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Olary Domain.||Strathearn Group.||||
72576|Dayana Formation|70405|5|Briefly described|p9 table 1, p32, p43 Table 3|Paleoproterozoic|Paleoproterozoic||1640 Ma - 1655 Ma|Mount Howden Subgroup||Overlies Mooleulooloo Formation, Correlates with Dalnit Bore Metasediments|Strongly schistose meta pelites.|
72576|Dayana Formation|70657|4|Described|p14-15, p24, p43|Statherian|Statherian|Occurs in the core of the Mount Howden Syncline, Olary Domain, Curnamona Province. Appears as the mis-spelt Dayanna Formation on p14 and p43. These authors claim that it was formerly the Dayanna Pelite of Conor (2000); this is wrong, as Conor (2000) presented the unit as the Dayana [sic] Pelite.|<1655 +/- 7 Ma|Mount Howden Subgroup||Overlies Mooleulooloo Formation. Equivalent to Dalnit Bore Metasediments in Broken Hill Domain.|Pale grey, fine-grained sillimanite-andalusite-staurolite schist.|
29486|Deep Creek Formation (SA)|42966|6|Mentioned|p179|||||||||
24241|Delisser Formation|22613|5|Briefly described|p25|||||||||
24241|Delisser Formation|22614|5|Briefly described|map|Pleistocene|Pleistocene|||||||
24241|Delisser Formation|40912|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
24241|Delisser Formation|42816|4|Described|p27|||||||||
24241|Delisser Formation|44133|5|Briefly described|p251|Quaternary|Quaternary|Aeolian sand. ||||||
24241|Delisser Formation|44695|5|Briefly described|Map Legend||Pleistocene|||||||
24241|Delisser Formation|69648|6|Mentioned|p33|||Sediments equivalent to older Delisser Formation on adjacent BARTON may also be present on OOLDEA.||||||
39171|Delken Member|24475|2|Defined|p52|Paleoproterozoic|Paleoproterozoic|Of Wandearah Formation. Overlain by Wokurna Member.||||||07-NOV-08
39171|Delken Member|65376|6|Mentioned|p101 Fig.3.1.|||||Unit in Wandearah Formation.||||
79319|Deuter Diorite|71129|5|Briefly described|p40-41|Statherian|Statherian|Geological Province: Gawler Craton.|1742+\-6 Ma (McAvaney and Jagodzinski 2012)|Unit of Moola Suite.||||
79319|Deuter Diorite|71862|2|Defined|p6-p7, p10, p22, p28-p30|Statherian|Statherian|Named after Deuter Paddock, Corunna Station, ~23km west of Iron Knob, Eyre Peninsula. This unit does not crop out and is only intersected in drillhole LED001 east of Lake Gilles. The type drillhole is DDH LED001 (229988), 680450mE, 6381003mN, GDA94, Zone 53 between 518.8-595m. This unit is an elliptical pluton that can be traced on magnetic imagery. This unit appears to cross cut the Cooyerdoo Granite and Sleaford Complex in TMI imagery. Geochemistry is discussed. See also p41-p42, p53, p55-p56, p58.|1742 +/- 6 Ma (McAveny and Jagodzinski, 2012)|Moola Suite||Intrudes the Wade Amphibolite. Intruded by dykes of the Gawler Range Volcanics.|Medium- to coarse-grained diorite composed of plagioclase and hornblende in a groundmass of biotite, pyroxene, K-feldspar and minor quartz which features xenoliths of amphibolite schist.|18-APR-23
74794|Devils Playground Volcanics|64722|6|Mentioned|p12|Neoarchean|Neoarchean|Gawler Province. Emplaced as part of igneous activity between 2650 and 2500 Ma.||||?Intrude Mulgathing Complex.||11-APR-12
74794|Devils Playground Volcanics|65376|5|Briefly described|pp10-11. |Archean|Archean|Oldest rocks in Gawler Craton. Low-grade metamorphism from c.2500-2400 Ma Sleafordian Orogeny.|2553 +/- 9 Ma.|||||
74794|Devils Playground Volcanics|65915|5|Briefly described|p2, p3 Fig.2, p18|Neoarchean|Neoarchean|In central northern Gawler Craton. 2553 +/- 9 Ma (Cowley and Fanning, 1991).||||||
74794|Devils Playground Volcanics|66302|5|Briefly described|p10-p12, p60, p61, p61 Fig.14, p85|||Christie and Wilgena Domains, Gawler Craton. Low grade metamorphism of this unit occurred between 2440-2420 Ma. Interpreted to have its origin in the same magmatic system as the Glenloth Granite, Coulta Granodiorite and the Hall Bay Volcanics.|2553 +/- 9 Ma (SHRIMP U-Pb, Fanning, 1997)|Mulgathing Complex|||Calc-alkaline andesite to rhyodacitic volcanics.|
74794|Devils Playground Volcanics|66520|2|Defined|p9-10, p15-18.  |Late Archean|Late Archean|Northern Gawler Craton. Reference drillhole: Eromanga Uranium Limited BKDDH01, 421-599 m. Strongly sericite and chlorite altered; thin carbonate veining common; sulfides sparse and sporadic.|2558 +/- 6 Ma (ID-TIMS U-Pb Zircon).|Mulgathing Complex.||Underlies Boorthanna Formation.|Green-grey basalt to andesite lava, breccia, lesser tuff; often porphyritic, locally amygdaloidal. Local intercalated pink-grey rhyodacite lava and tuff, occasionally porphyritic or spherulitic. Greenschist-facies metamorphosed.|
74794|Devils Playground Volcanics|66882|5|Briefly described|p116|Neoarchean|Neoarchean|Central Gawler Craton. Possible source of sediments (and zircons) for Cook Gap Schist. Calc-alkaline rocks.|c.2560 Ma|||||
74794|Devils Playground Volcanics|66916|6|Mentioned|p9|Paleoproterozoic|Archean|Basement N of Olympic Dam.|c.2555 Ma.|||||
74794|Devils Playground Volcanics|67058|5|Briefly described|p476, p492, p493.|Neoarchean|Neoarchean|Central Gawler Craton. Contains significant negative Eu anomalies: may be a source for the Eba Formation.|c.2550 Ma (Swain et al. 2005).|Unit in Mulgathing Complex.||||15-MAR-12
74794|Devils Playground Volcanics|67721|5|Briefly described|p36|Neoarchean|Neoarchean||c. 2530 Ma (Fanning, Reid and Teale 2007)|Of the Mulgathing Complex.||||
74794|Devils Playground Volcanics|68128|5|Briefly described|p6,7|Neoarchean|Neoarchean|Also Devils Playground volcanics  Table 2 p6, and Devil's Playground volcanics p5.|2553 +/- 9 Ma (ID-TIMS U-Pb)mag crystallisation|Of Mulgathing Complex? ||||
74794|Devils Playground Volcanics|68208|6|Mentioned|p31 Fig.2|Neoarchean|Neoarchean||Crystallisation age ~2560 Ma|Of Mulgathing Complex||||
74794|Devils Playground Volcanics|70027|6|Mentioned|p71|Neoarchean|Neoarchean|Geological province: Gawler Craton. Possible source of ca. 2560 Ma magmatic rocks in the Mulgathing Complex.|ca. 2555 Ma|||||
74794|Devils Playground Volcanics|71043|5|Briefly described|p105-108, p115, p117|Neoarchean|Neoarchean|Olympic Cu-Au Province, Gawler Craton. Known from only three drillholes. Calc-alkaline affinity; active margin subduction setting. Significance of the adularia veins discussed.|2553 +/- 5 Ma (SHRIMP zircon: this study).|Mulgathing Complex.|||Andesite, dacite, dacite tuff, trachyte, basalt. Minor (greenschist) metamorphic grade. Marked by adularia-bearing quartz - calcite (+chlorite - chalcopyrite - pyrite) veins.|
74794|Devils Playground Volcanics|71322|5|Briefly described|p100||||c.2555 Ma.|||||
74794|Devils Playground Volcanics|71534|5|Briefly described|p299|Neoarchean|Neoarchean|Geological province: Gawler Craton. Primitiva basaltic rock composition enriched in LILE elements, while depleted in Nb and Ta; likely associated with mantle-dominated magmatism in an extensional continental magmatic arc (Redi et al., 2009b; Swain et al., 2005).|c. 2555 Ma|||||
74794|Devils Playground Volcanics|71536|5|Briefly described|p1, p3, p119, p127, p129, p215|Neoarchean|Neoarchean|A 2553 +/- 5 Ma SHRIMP age is derived in this volume and interpreted as the age of magmatic crystallisation. Rb-Sr and Sm-Nd isotopic work from Swain et al., 2005 and Reid et al., 2009 respectively confirm an Archean age (exact dates not provided).|c. 2558 +/- 6 Ma (ID TIMS)||||Andesitic and basaltic volcanic rocks.|
74794|Devils Playground Volcanics|73030|6|Mentioned|p2149-2151|Neoarchean|Neoarchean|Gawler Craton, Olympic Cu-Au Province. Located only in the eastern Gawler Craton in the northern region of the Olympic Cu-Au province. Have undergone only lower greenschist-facies metamorphism.|ca. 2555 Ma||||Includes felsic volcanics.|
74794|Devils Playground Volcanics|73092|6|Mentioned|p35|Archean|Archean|Gawler Craton.||||||
74794|Devils Playground Volcanics|73230|4|Described|p4, p6-7, p10, p12|Neoarchean|Neoarchean|Gawler Craton. Domain: Eastern Mulgathing Complex. Metamorphosed to greenschist facies. Pervasive chlorite and sericite alteration. Potential for volcanic-related sulfide and/or epithermal gold mineralisation because the unit may represent convergent margin volcanics.|c. 2553 Ma (magmatic)|Mulgathing Complex|||Bimodal calc-alkaline volcanics, metamorphosed to greenschist facies.|
34532|Dey-Dey Mudstone|22746|4|Described|Fig.3 p515, p521|Neoproterozoic III|Neoproterozoic III|||||||
34532|Dey-Dey Mudstone|23287|6|Mentioned|p104|||||||||
34532|Dey-Dey Mudstone|23524|5|Briefly described|p221 Fig. 3|Neoproterozoic|Neoproterozoic|||||||
34532|Dey-Dey Mudstone|63397|2|Defined|Map Legend|Neoproterozoic III|Neoproterozoic III|Of the Ungoolya Group. Type section in text. Red-brown with some green-grey silty mudstone, dolomitic/calcareous siltstone/mudstone, conglomerate. Thickness: 900m. Overlies: Murnaroo Formation. Underlies: Karlaya Limestone Member, Tanana Formation||||||24-MAR-21
34532|Dey-Dey Mudstone|68271|5|Briefly described|p697|||Officer Basin. Ediacaran correlative to Bunyeroo Formation.||||||
34532|Dey-Dey Mudstone|73392|6|Mentioned|p3||||||||Sampled from core of Giles 1 well.|
33818|Diamond Bog Dolomite|63056|5|Briefly described|p79, p81 Fig. 2|Early Cambrian|Early Cambrian|Comprises dolomite with vuggy and mouldic porosity. Thickness: >120m. Geological Province: Warburton Basin. Potentially significant reservoir.||||||06-FEB-07
33818|Diamond Bog Dolomite|65489|5|Briefly described|p39, p96, p119-120|Middle Cambrian|Middle Cambrian|Eastern Warburton Basin. Potentially significant reservoir.||||Is overlain unconformably by Kalladeina Formation.|Dolostone with vuggy and moldic porosity.|
33818|Diamond Bog Dolomite|67402|4|Described|p239, p261|Early Cambrian|Early Cambrian|Warburton Basin. Unsuitable reservoir for the storage of carbon dioxide as it contains low porosity and permeability. Deposited in a high stand setting. 120m thick.||||Overlain by the Kalladeina Formation. Unconformably overlies the Mooracoochie Volcanics.|Dolomite with vuggy and mouldic porosity.|
33818|Diamond Bog Dolomite|67536|6|Mentioned|Map Legend|||Warburton Basin.|||||Vuggy dolomite.|01-APR-14
33818|Diamond Bog Dolomite|68731|5|Briefly described|p168, p170 Fig 3.83|Middle Cambrian|Middle Cambrian|> 120 m thick. Potentially significant reservoir; recovered heavily gas cut salt water from this fractured unit; carbonate disconformity overlies volcanics.||||Unconformably underlain by the Mooracoochie Volcanics. Unconformably overlain by the Kalladeina Formation.||
33818|Diamond Bog Dolomite|69982|3|Fully described|p17, p22, p42, p45, p51, p53-54, p56|Middle Cambrian|Middle Cambrian|See also p82-85, p147-148, p223. New name. Type section is the interval 2440 - 2546 m in Gidgealpa 5 core. Over 150m thick. A target for gas during exploration in the 1950s and 1960s. Warburton Basin. Reservoir attributes described. Brief thin section descriptions. Composite logs shown. Details of wells with hydrocarbon shows.||||Overlies Mooracoochie Volcanics or Jena Basalt. Is overlain by the Kalladeina Formation. May correlate with Wirrealpa Limestone (Arrowie Basin).|Vuggy dolomite, from complete dolomitisation and karstification of an oncoid-intraclastic wackestone and packstone.|
33818|Diamond Bog Dolomite|73244|6|Mentioned|p86|Cambrian|Cambrian|Warburton Basin. Shallow shelf environment. Gas.||||||
33818|Diamond Bog Dolomite|73479|5|Briefly described|p156|Cambrian|Cambrian|Warburton Basin. Shallow shelf depositional environment.|ca 510 Ma|||Unconformably overlies Mooracoochie Volcanics, underlies Kalladeina Formation||
24247|Dome Sandstone|22772|5|Briefly described|Table13.1|Cryogenian|Cryogenian|||||||
24247|Dome Sandstone|22857|5|Briefly described|Tb. 13.1 (insert p70-71)|Willouran|Willouran|Of the Curdimurka Subgroup ( Callanna Group).||||||
24247|Dome Sandstone|23054|6|Mentioned|p11|||||||||
24247|Dome Sandstone|24175|3|Fully described|p9|Neoproterozoic|Neoproterozoic|Of Curdimurka Subgroup. Overlain by Rook Tuff.  Max. thickness in type section: 1480m. Age is Late Willouran in South Australian chronostratigraphic time scale).||||||13-FEB-08
24247|Dome Sandstone|24321|5|Briefly described|Map legend|Adelaidean|Adelaidean|Parent: Curdimurka Subgroup.||||||
24247|Dome Sandstone|37854|2|Defined|p9|Adelaidean|Adelaidean|Prob.Late Willouran||||||
24247|Dome Sandstone|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Willouran||||||
24247|Dome Sandstone|40294|6|Mentioned|p9|||||||||
24247|Dome Sandstone|41402|6|Mentioned|p42|||||||||
24247|Dome Sandstone|41403|4|Described|p61|||||||||
24247|Dome Sandstone|41404|6|Mentioned|p73|||See also P89||||||
24247|Dome Sandstone|42087|5|Briefly described|Fig.2 P15|||||||||
24247|Dome Sandstone|42222|5|Briefly described|p11|||||||||
24247|Dome Sandstone|42223|6|Mentioned|p42|||||||||
24247|Dome Sandstone|42238|5|Briefly described|Table 1 P75|||||||||
24247|Dome Sandstone|43052|5|Briefly described|p175,Table 6.1|||Of Curdimurka Subgroup.||||||13-FEB-08
24247|Dome Sandstone|44289|5|Briefly described|Map Legend||Neoproterozoic|||||||
24247|Dome Sandstone|60718|5|Briefly described|p49 Fig. 2, P50, 52|Adelaidean|Adelaidean|1500m thick. Geological Province: Adelaide Geosyncline.||Of Curdimurka Subgroup (Callanna Group).||Unconformably underlies Rook Tuff.||15-APR-11
24247|Dome Sandstone|64796|6|Mentioned|p190 Fig.8|Neoproterozoic|Neoproterozoic|Appears in Fig.8 without the lithology.||Unit in Curdimurka Subgroup.||Overlies Noranda Volcanics (Arkaroola Subgroup). Is overlain by Rook Tuff.||
24247|Dome Sandstone|72492|6|Mentioned|p2 Fig.1, p3, p5 Fig.4e|Neoproterozoic|Neoproterozoic|In Willouran Ranges.||Curdimurka Subgroup||Unconformably underlies Dunns Mine Limestone and underlies Rook Tuff.|Includes crossbeds, halite casts and channel conglomerate.|
24247|Dome Sandstone|73222|6|Mentioned|p7|Tonian|Tonian|Willouran Ranges. Torrensian.||Curdimurka Subgroup, Callanna Group, Warrina Supergroup||Underlain by Noranda Volcanics (Arkaroola Subgroup). Overlain by Rook Tuff.||
24247|Dome Sandstone|74367|5|Briefly described|p7 Fig.6, p8-9, p12-14, p16, p20|Tonian|Tonian|Detrital zircon MDA is older than the true depositional age based on maximum and minimum age constraints from the Wooltana Volcanics (830+/-50 Ma) and Rook Tuff (802+/-10 Ma).|993+/-62 Ma LA-ICP-MS detrital zircon MDA|Curdimurka Subgroup||||
39166|Doora Member|24475|2|Defined|p50|Paleoproterozoic|Paleoproterozoic|Of Wandearah Formation. Formerly Doora Schist and Doora Metasediments, both now abandoned.||||||07-NOV-08
39166|Doora Member|60958|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Wandearah Formation.  Biotitie schist-dominated unit. Layered, foliated biotite-rich schist of psammitic, argillaceous, calcsilicate, iron rich, graphitic and minor albitic meta-sediments. Age: 1741 +/- 9Ma. Geological Province: Gawler Craton.||||||07-NOV-08
39166|Doora Member|61121|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Wandearah Formation. Biotite schist-dominated unit. Layered, foliated, biotite-rich schist of psammitic, argillaceous, calcsilicate, iron-rich graphitic and minor albitic metasediments.  Age: ~1741+/-9Ma. Geological Province: Gawler Craton.||||||07-NOV-08
39166|Doora Member|63398|5|Briefly described|p672|||Of the Wandearah Formation. Metasediments. ||||||
39166|Doora Member|65375|4|Described|p19, p21, p47.|Paleoproterozoic|Paleoproterozoic|Formerly Doora Schist (Parker 1980); Doora Metasediments (Conor 1995). Multiply (three generations) deformed. Doora Member schist hosts copper mineralisation in Kadina area.||Unit in Wandearah Formation.||Interdigitates with, and locally overlies, Moonta Porphyry. Intruded by Tickera and Arthurton Granites. Is overlain by Wokurna Member and locally by Winulta Formation.|Layered, foliated, biotite-rich schistose, psammitic, pelitic, calc-silicate, iron rich, graphitic and minor albitic metasediments.|
39166|Doora Member|65376|5|Briefly described|p101, p104, p109. |||Formerly Doora Schist. Its age may be slightly older than that of the intercalated Moonta Porphyry Member (c.1750 Ma).||Unit in Wandearah Formation.||Intruded by Moonta Porphyry Member.|Schistose, medium-grained, thinly planar to laminated quartz-plagioclase-bearing metasediments, commonly iron-rich; also calcsilicate, biotite-quartz-albite pelite, quartz-albite-magnetite-biotite iron formation; minor marble and quartz albitite.|
39166|Doora Member|66302|5|Briefly described|p29|Statherian|Statherian|Ages are U-Pb dates from Fanning et al. (2007).|1753 +/- 8 Ma to 1748 +/- 15 Ma|Weetulta Formation||Intercalated with the Moonta Porphyry Member.|Pelitic to psammitic mica schist, hornfels, amphibolite and iron formation.|
39166|Doora Member|69748|6|Mentioned|p179-181, 183|Paleoproterozoic|Paleoproterozoic|Moonta-Wallaroo region, Olympic IOGC Province.||Wandearah Formation.|||Albite-biotite schists.|
39166|Doora Member|70382|6|Mentioned|p33|||Possible source for some of Quartoo Sand Member inherited zircon.|~1740 Ma|Unit of Weetulta Formation.||||
38055|Dugong Supersequence|23792|5|Briefly described|p47, Fig.D4|||Equivalent to Wilsons Bluff Limestone. Geological Province: Bight Basin. Off shore. See also Dugong supersequence.||||||15-JUN-05
38055|Dugong Supersequence|24336|5|Briefly described|p99 Fig.3||Lutetian|Correlated to the Nullabor Limestone and Wilson Bluff Limestone.||||||
38055|Dugong Supersequence|61544|6|Mentioned|p367 Fig.3. |Eocene|Eocene|Ceduna Sub-basin. Post-break-up thermal subsidence.||||Overlies Wobbegong Supersequence.||
38055|Dugong Supersequence|66578|6|Mentioned|p1007 Fig.4, p1010.|Quaternary|Paleogene|Ceduna Sub-Basin, Bight Basin.||||Overlies Wobbegong Supersequence.||
38055|Dugong Supersequence|69297|6|Mentioned|p14 fig 2.4, p25 fig 2.9|Tarantian|Ypresian|Eyre, Ceduna and Duntroon Sub-basins. Marls may be adequate sealing units. See also p26 fig 2.11, p43, p60,p61, p64.  ||||Overlies the Wobbegong Supersequence.|Includes marl and limestone.|
38055|Dugong Supersequence|70067|5|Briefly described|Ceduna: Fig.2. Regional: Fig.2; p5|Holocene|Lutetian|Bight Basin. Comprises Nullarbor and Wilsons Bluff Limestones. Thick basal transgressive marls form a regional seal (for Hammerhead and Wobbegong Supersequences).||||Overlies Wobbegong Supersequence.|Includes marls and limestones.|
24255|Dullingari Group|13497|5|Briefly described|ix, p75, p114, p179, p191|Ordovician|Ordovician|Warburton Basin. Commonly mistaken as Merrimelia Formation rocks. Hosts rare graptolite fossils.  |||||Black shale.|
24255|Dullingari Group|22527|6|Mentioned|p 1|||||||||
24255|Dullingari Group|22650|6|Mentioned|p 160||Ordovician|Province - Warburton Basin.||||||
24255|Dullingari Group|22883|5|Briefly described|Fig2 P30|Devonian|Cambrian|||||||
24255|Dullingari Group|23054|6|Mentioned|p36|||||||||
24255|Dullingari Group|23154|5|Briefly described|Map Legend|Ordovician|Ordovician|Geological Province - Warburton Basin.||||||
24255|Dullingari Group|23155|5|Briefly described|p9|Ordovician||Geological Province - Warburton Basin. The unit is informally divided into upper and lower Dullingari Group but no separate formations have been defined.||||||
24255|Dullingari Group|38661|2|Defined|p7|Late Ordovician|Early Ordovician|Early to early Late Ordovician.||||||
24255|Dullingari Group|40642|4|Described|p171|||Mention p169.||||||04-APR-07
24255|Dullingari Group|40830|6|Mentioned|p8|||||||||
24255|Dullingari Group|41288|6|Mentioned|Fig.7|||||||||
24255|Dullingari Group|42064|4|Described|p166|||||||||
24255|Dullingari Group|42357|5|Briefly described|p10|||||||||
24255|Dullingari Group|42746|4|Described|p3, Fig.2 p5|||||||||
24255|Dullingari Group|43052|5|Briefly described|Table 2.1|||||||||
24255|Dullingari Group|43213|6|Mentioned|p63|Ordovician|Ordovician|Warburton Basin. Described by Gatehouse (1986) who pointed out the lithological similarity between this unit and most basement cores from the Thomson Fold Belt.||||||
24255|Dullingari Group|43570|6|Mentioned|Fig.2,p535|Ordovician|Cambrian|||||||
24255|Dullingari Group|44133|5|Briefly described|p43, 33-34, 4 Fig. 7.2|Late Ordovician|Early Ordovician|Geological Province: Western-Eastern Warburton Basin. ||||||
24255|Dullingari Group|44289|5|Briefly described|Map Legend|Ordovician|Late Cambrian|||||||
24255|Dullingari Group|63056|5|Briefly described|p80, p81 Fig. 2|Early Ordovician|Early Ordovician|Includes black shales with rare graptolites. Thickness: >770m. Geological Province: Warburton Basin. Slope (dark grey shale and lime mudstone, slump breccia) and basinal shale, siltstone and thin spicular chert, pyritic; graptolites, acritarchs.||||||06-FEB-07
24255|Dullingari Group|63224|5|Briefly described|p9|||Geological Province: Warburton Basin.||||||07-FEB-08
24255|Dullingari Group|63978|5|Briefly described|p5|Middle Ordovician||Both Kalladeina (upper part) and Innamincka Formations pass laterally into this group. Geological province: Warburton Basin. Comprises turbiditic quartzose sandstone, shale and siltstone.||||||07-FEB-11
24255|Dullingari Group|65489|5|Briefly described|p28, p30, p96, p119-121|Late Cambrian|Middle Cambrian|Gatehouse (1983). Eastern Warburton Basin. Most units have undergone only low-grade metamorphism. Mis-spelt as both Dullinggari and Dillingari on p120.|||Includes Lycosa, Narcoonowie Formations.||Slope (dark grey shale and lime mudstone, slump breccia) and basinal graptolitic black shale, siltstone and thin spicular chert, pyritic; rare conglomerate intervals.|
24255|Dullingari Group|65925|5|Briefly described|Appendix 2.||||||||Black pyritic shale; grey, white sandstone; grey, green mudstone.|
24255|Dullingari Group|66623|6|Mentioned|p101.|||Warburton Basin. Possible correlative to Easter Monday Formation of Koonenberry Belt.||||||
24255|Dullingari Group|67402|4|Described|p260, p261|Bolindian|Lancefieldian|Warburton Basin. Deposited in deep water environments. ||||Grades laterally into the Kalladeina and Innamincka Formations. Overlies the Pando Formation.|Black shales and minor siltstones.|
24255|Dullingari Group|67536|6|Mentioned|Map Legend|||Warburton Basin.|||||Slope to basinal shale, siltstone, lime mudstone; minor sandstone and pebbly sandstone at top.|
24255|Dullingari Group|68068|5|Briefly described|Map legend|Middle Ordovician|Middle Cambrian|Warburton Basin. Age from graptolites in shale facies. Marine outer shelf and deep basin.|||||Dark grey to black shale, laminated, pyritic, variably calcareous, interbedded locally with cream spiculitic chert, siltstone and fine- to coarse-grained lithic sandstone, conglomeratic in part.|
24255|Dullingari Group|68731|6|Mentioned|p115, p119, p164, p168, p170 Fig 3.83|Ordovician|Ordovician|Warburton Basin. See also misspelt Dullinggari Group and Dillingari Group, all p170.||||Basinal shale interfingers with the Kalladeina Formation.|Comprises turbiditic quartzose sandstone, shale, and siltstone. Several basalt units occur within this succession.|17-DEC-13
24255|Dullingari Group|69023|5|Briefly described|p78-80, p191-192|Ordovician|Middle Cambrian|Defined as all rocks of known or presumed Ordovician age in the Warburton Basin (Gatehouse 1983,1986). The lower part of this unit correlates with uppermost Kalladeina Formation and all of the Innamincka Formation. Type section is in Dullingari 1 core. Stratigraphic wells intersection data.|||||Drab-grey siltstone with minor interbeds of very micaceous, arkosic, calcite-cemented sandstone; above that is 0.2m thick pebbly conglomerate in a sandy arkosic matrix; at top are thin interbeds and lenses of dark grey siltstone and shale.|
24255|Dullingari Group|69449|5|Briefly described|p34:2 Fig.34.2|Cambrian|Cambrian|Eastern Warburton Basin.||||Overlies Kalladeina Formation. Is overlain by Innamincka Formation.||12-JUL-16
24255|Dullingari Group|69673|6|Mentioned|p149 fig 120|||||||||
24255|Dullingari Group|69982|3|Fully described|p23-29, p10, p13-14, p17-19, p45, p47|Early Ordovician|Early Ordovician|See also p145, p170, p220, p223-224, Appendix 1. Gatehouse (1983), who nominated a type section from 2758.1 to 3532.5 m in Dullingari 1 core. Warburton Basin. A turbidite depositional mechanism is suggested. Fossils used for determining the age of the Group are disputed. Hosts 22% of the oil, and 60% of gas, shows in the Basin. Brief thin section descriptions. Composite log shown. Bedding dip angles in wells listed. Details of wells with hydrocarbon shows. Mis-spelt as Dullingiari on p220.|||Includes Lycosa, Narcoonowie and Kalladeina Formations.|Is overlain unconformably by Toolachee Formation.|Includes pyritic shale, siltstone; minor highly indurated sandstone, and glauconitic bioturbated sandstone to conglomerate or breccia, and siltstone.|12-NOV-15
24255|Dullingari Group|70749|5|Briefly described|p43, p54|Ordovician|Cambrian|Warburton Basin.||||Is overlain by Pando Formation.|Deeper water slope and basinal shales and/or turbidites.|
24255|Dullingari Group|70823|5|Briefly described|p35|Ordovician|Cambrian|Warburton Basin. Deposited in a deep marine environment.|||||Shale, siltstone and chert.|
24255|Dullingari Group|71283|5|Briefly described|p471, p472 Fig.2|Ordovician|Cambrian|Gatehouse (1983, 1986). Warburton Basin.|||||Pyritic shale, siltstone and minor sandstone, with a high degree of induration, probably at the zeolite grade of metamorphism. Also includes glauconitic bioturbated sandstone and siltstone.|
24255|Dullingari Group|71342|6|Mentioned|Ch9 p11, Ch10 p20|Ordovician|Ordovician|Warburton Basin.||||||
24255|Dullingari Group|71965|5|Briefly described|p898|||Geological province: Thomson Orogen. Of Warburton Basin.|||Includes Lycosa Formation.|Correlable to Warratta Group.||
25887|Dunns Mine Limestone|22772|5|Briefly described|Table13.1|Cryogenian|Cryogenian|||||||
25887|Dunns Mine Limestone|22857|5|Briefly described|Tb. 13.1 (insert p70-71)|Willouran|Willouran|Of the Curdimurka Subgroup (Callanna Group).||||||
25887|Dunns Mine Limestone|23054|6|Mentioned|p11|||||||||
25887|Dunns Mine Limestone|23314|5|Briefly described|331 Fig.2|||||||||
25887|Dunns Mine Limestone|24175|3|Fully described|p9|Neoproterozoic|Neoproterozoic|Of Curdimurka Subgroup. Overlies Rook Tuff; underlies Recovery Formation.  Max. thickness: 334m.||||||13-FEB-08
25887|Dunns Mine Limestone|24321|5|Briefly described|Map legend|Adelaidean|Adelaidean|Parent: Curdimurka Subgroup.||||||13-FEB-08
25887|Dunns Mine Limestone|37854|2|Defined|p10|Adelaidean|Adelaidean|Prob.Late Willouran||||||
25887|Dunns Mine Limestone|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Willouran||||||
25887|Dunns Mine Limestone|40294|6|Mentioned|p9|||||||||
25887|Dunns Mine Limestone|41402|6|Mentioned|p42|||||||||
25887|Dunns Mine Limestone|42222|5|Briefly described|p11|||||||||
25887|Dunns Mine Limestone|42238|5|Briefly described|Table 1 P75|||||||||
25887|Dunns Mine Limestone|43052|5|Briefly described|p175,Table 6.1|||of Curdimurka Subgroup.||||||
25887|Dunns Mine Limestone|60718|5|Briefly described|p49 Fig. 2, p50|Adelaidean|Adelaidean|Geological Province: Adelaide Geosyncline.||Of Curdimurka Subgroup (Callanna Group).||||15-APR-11
25887|Dunns Mine Limestone|64793|6|Mentioned|p285 fig 4|||Adelaide Rift Complex.||Unit in Callanna Group.||||
25887|Dunns Mine Limestone|64796|6|Mentioned|p190 Fig.8, p194 Tb.2, p200 Fig.10, p202|Neoproterozoic|Neoproterozoic|Willouran Ranges. Appears in Fig.8 without the lithology.||Unit in Curdimurka Subgroup.||Overlies Rook Tuff. Is overlain by Recovery Formation.||
25887|Dunns Mine Limestone|64797|6|Mentioned|p161 Tb.4|||Adelaide Rift Complex. Lithology/rank not shown on diagram. S-isotope data. ||||||
25887|Dunns Mine Limestone|72492|5|Briefly described|p2 Fig.1, p3, p7 Tb.1, p10 Tb.2|Neoproterozoic|Neoproterozoic|In Willouran Ranges. Misspelt on p7 Tb.1 as 'Dunns mine limestone'. Also Dunns Limestone p2, p3. See also p11 Tb.3.||Curdimurka Subgroup||Overlies Rook Tuff and underlies Recovery Formation.|Includes crossbeds, halite casts and halite casts.|
25887|Dunns Mine Limestone|73222|5|Briefly described|p6-7|Tonian|Tonian|Willouran Ranges. Torrensian. One of few carbonate units within the Callanna Group. Slightly younger than Waraco Limestone. Thickness: 50 to 200 m. Chalcedonic nodules are found in the lower part of the section.||Curdimurka Subgroup, Callanna Group, Warrina Supergroup||Underlain by Rook Tuff. Unconformably overlain by Recovery Formation. Possibly equivalent to Wirrawilka Beds.|Dark grey dolostone interbedded with beds of calcareous shale and siltstone and lenses of sandstone.|
23568|Ealbara Rhyolite|23490|5|Briefly described|p22||Mesoproterozoic|Of Gawler Range Volcanics, Gawler Craton.||||||
23568|Ealbara Rhyolite|38604|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
23568|Ealbara Rhyolite|38605|6|Mentioned|p15|||||||||
23568|Ealbara Rhyolite|39802|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
23568|Ealbara Rhyolite|39905|6|Mentioned|Fig.4|||||||||
23568|Ealbara Rhyolite|40644|6|Mentioned|p124 Fig. 3|Mesoproterozoic|Paleoproterozoic|Age: 1510+/-15Ma (see Table 4, p135).||||||07-NOV-08
23568|Ealbara Rhyolite|41972|6|Mentioned|Table 3 P378|||||||||
23568|Ealbara Rhyolite|41995|6|Mentioned|p16|||||||||
23568|Ealbara Rhyolite|42465|5|Briefly described|Map Legend|||||||||
23568|Ealbara Rhyolite|42469|4|Described|p16|||||||||
23568|Ealbara Rhyolite|42546|5|Briefly described|Map legend|Mesoproterozoic||||||||
23568|Ealbara Rhyolite|42736|5|Briefly described|map legend|Mesoproterozoic||||||||
23568|Ealbara Rhyolite|43052|5|Briefly described|p113|||Of Gawler Range Volcanics.||||||02-JUN-09
23568|Ealbara Rhyolite|44935|5|Briefly described|Map Legend||Proterozoic|||||||
23568|Ealbara Rhyolite|50605|5|Briefly described|p(ii), 8.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Gawler Craton and Curnamona Province. Of the Lower Gawler Range Volcanics. Age: 1589 +/- 16Ma (U-Pb).||||||02-JUN-09
23568|Ealbara Rhyolite|65376|6|Mentioned|p203.|||Occurs near Bulgunnia Homestead.|||||Interlayered with sandstones.|
23568|Ealbara Rhyolite|66302|6|Mentioned|p33, p45|Calymmian|Calymmian||1589 +/- 16 Ma (U-Pb, Fanning, 1997)|Gawler Range Volcanics||||
23568|Ealbara Rhyolite|68128|5|Briefly described|p53|Mesoproterozoic|Mesoproterozoic|Gawler Craton.|||||Flow-banded, rhyolite; rhyodacite, ignimbrite, tuff.|31-JAN-23
23568|Ealbara Rhyolite|68131|6|Mentioned|p77|Mesoproterozoic|Mesoproterozoic|||||||
23568|Ealbara Rhyolite|70659|5|Briefly described|p5-6, p8|Mesoproterozoic|Mesoproterozoic|Greater than 2km thick succession, with a total area of 2000 km2.||Lower Gawler Range Volcanics.||Intercalated with Konkaby Basalt in places.|Densely-welded crystal- and lithic-rich ignimbrite interlayered with massive porphyritic rhyolite and lesser rhyodacite and dacite.|06-FEB-17
23568|Ealbara Rhyolite|70816|6|Mentioned|p4-5|||Tarcoola-Kingoonya area, Gawler Ranges.||Unit of lower Gawler Range Volcanics.||||
23568|Ealbara Rhyolite|72090|6|Mentioned|p11-p12|||Gawler Craton.|1590.3 +/- 0.5 Ma|Gawler Range Volcanics, Lower||||
23568|Ealbara Rhyolite|72459|6|Mentioned|p51|Palaeoproterozoic|Palaeoproterozoic||1589 +/- 17 Ma|||||
23568|Ealbara Rhyolite|73110|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|||Lower Gawler Range Volcanics.||||
34326|Eba Formation|22629|6|Mentioned|fig1p146,157|Proterozoic|Proterozoic|Formally assigned to the Tarcoola Formation||||||
34326|Eba Formation|23481|5|Briefly described|p19 Fig 1|||Geological Province: Gawler Craton.||||||
34326|Eba Formation|23805|5|Briefly described|p4 Fig. 1|Paleoproterozoic|Paleoproterozoic|Geological Province: Gawler Craton.||||||07-NOV-08
34326|Eba Formation|24422|6|Mentioned|p84 Fig. 1|||Geological Province: Gawler Craton.||||||
34326|Eba Formation|24472|5|Briefly described|p5 Tb.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Harris Greenstone Domain, Gawler Craton. Age: ~1740 Ma.||||||07-NOV-08
34326|Eba Formation|24505|5|Briefly described|p5 Fig. 1|||Geological Province: Gawler Craton.||||||
34326|Eba Formation|24597|5|Briefly described|p526 Fig. 1|Paleoproterozoic|Paleoproterozoic|Geological Province: Gawler Craton.||||||07-NOV-08
34326|Eba Formation|60515|6|Mentioned|p116 Fig.1 |||||||||
34326|Eba Formation|60953|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Age: >1723Ma. Quartzite, siltstone, shale, minor basalt.||||||07-NOV-08
34326|Eba Formation|60954|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Geological Province: Gawler Craton.||||||31-MAY-05
34326|Eba Formation|61108|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|Quartzite, siltstone, shale and minor basalt. Age: >1723 Ma.||||||07-NOV-08
34326|Eba Formation|61522|5|Briefly described|p5 Fig.1|||Geological Province: Gawler Craton.||||||
34326|Eba Formation|61864|6|Mentioned|p16 fig 3|||||||||
34326|Eba Formation|63866|6|Mentioned|p9, p30|||||||||
34326|Eba Formation|64130|6|Mentioned|p1378 Fig.1, p1380 Fig.2, p1382|Paleoproterozoic|Paleoproterozoic|Central Gawler Craton.|~1715 Ma||||Basal conglomerate overlain by quartzites and black shale packages with basaltic and felsic volcanic rocks.|
34326|Eba Formation|64722|6|Mentioned|Fig. 5 p.13|Proterozoic|Proterozoic|Of South Australian Craton.||||||
34326|Eba Formation|64739|6|Mentioned|p264 Fig.1.|||Gawler Craton.||||||
34326|Eba Formation|64828|5|Briefly described|p1064 Fig. 1|Mesoproterozoic|Paleoproterozoic|Geological province: Gawler Craton.||||||04-MAR-09
34326|Eba Formation|65376|6|Mentioned|p8 Fig.1.1. ||||c.1715 Ma.|||||
34326|Eba Formation|65390|6|Mentioned|p11 Fig.1, p22 Fig. 3|Statherian||Wilgena Domain, Gawler Craton. Age >1720 Ma.||||||
34326|Eba Formation|65485|6|Mentioned|Fig 1|Paleoproterozoic|Paleoproterozoic|||||||19-MAR-12
34326|Eba Formation|65922|6|Mentioned|p13 Fig. 4|||Gawler Craton.||||||
34326|Eba Formation|66302|5|Briefly described|p4 Fig.3, p22, p32, p76 Fig.20|Statherian|Statherian|Wilgena Domain, Gawler Craton. Deposited in a high to moderate energy fluvial or shallow marine environment.|ca. 1740-1710 Ma|||Unconformably overlain by the Labyrinth Formation.|Thick-bedded, white quartzite, siltstone, shale and sandstone that is interbedded with amygdaloidal basalt.|
34326|Eba Formation|67058|3|Fully described|pp476-478, p481 Fig.5, pp482-497.|Paleoproterozoic|Paleoproterozoic|Central Gawler Craton. Deposited in a high- to moderate-energy fluvial or shallow marine environment. Its geochemistry is discussed in detail. Authors discuss possible sediment sources, arguing for erosion of Archean material and demonstrating similarities with the Sleaford and Mulgathing Complexes. Also presented as Mount Eba Formation in this article (presented as Mt in text).|Max. 2538 +/- 9 Ma (this study).|||Is overlain unconformably by Labyrinth Formation.|Thick-bedded, clean, white quartzites with abundant granules and pebbles, then a less mature quartzite, overlain by siltstones and shales transitioning through sandstone back to an overlying pure white quartzite.|15-MAR-12
34326|Eba Formation|67323|5|Briefly described|Eastern Australia Time-Space Plot; p33|||Central Gawler Craton.|1715 +/- 9 Ma.||||Coarse clastic succession.|
34326|Eba Formation|67536|5|Briefly described|Map Legend|Statherian|Statherian|Gawler Craton.|||||Quartzite, siltstone, shale, minor basalt.|
34326|Eba Formation|69004|6|Mentioned|p18|||Gawler Craton.||||||
34326|Eba Formation|69649|6|Mentioned|p6 Fig.4,|||||||||
34326|Eba Formation|71341|6|Mentioned|p188 fig 7|||||||||
34326|Eba Formation|72459|6|Mentioned|p51|Palaeoproterozoic|Palaeoproterozoic|Wilgena, depoisted in shallow localised basins.|ca. 1730-1700 Ma|||||
25716|Edeowie Limestone Member|35255|6|Mentioned|p32|||||||||
25716|Edeowie Limestone Member|35395|1|Redefined|p101|Early Cambrian|Early Cambrian|||||||
25716|Edeowie Limestone Member|35835|6|Mentioned|p198|||Now part of Oraparinna Shale Moore(1979)||||||
25716|Edeowie Limestone Member|36244|6|Mentioned|p2|||Defined by Moore 1979.||||||
25716|Edeowie Limestone Member|36495|6|Mentioned|p117|||||||||
25716|Edeowie Limestone Member|42011|6|Mentioned|p459|||||||||
25716|Edeowie Limestone Member|42213|6|Mentioned|p474|||||||||
25716|Edeowie Limestone Member|42222|6|Mentioned|p20|||||||||
25716|Edeowie Limestone Member|42573|5|Briefly described|Fig.2 P191|||||||||
25716|Edeowie Limestone Member|44133|5|Briefly described|p23, 26-27|||Of the Oraparinna Shale. Onlaps lower Wilkawillina Limestone.||||||
25716|Edeowie Limestone Member|60418|5|Briefly described|p135|Early Cambrian|Early Cambrian|Of Billy Creek Formation. Geological Province: Arrowie Basin of Adelaide Geosyncline||||||
25716|Edeowie Limestone Member|60889|5|Briefly described|p245 Fig.2, p247 Fig.4, p249 Fig.6|Early Cambrian|Early Cambrian|Shown as Edeowie Limestone Mbr (Fig.2), Edeowie Mbr (Fig.4) and Edeowie Limestone (Fig.6). Arrowie Basin.||Billy Creek Formation||Overlies Moorowie Formation.||21-SEP-17
25716|Edeowie Limestone Member|60959|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of the Billy Creek Formation. Planar to wavy laminated, platy dolomite mudstone with peloidal sandy limestone and tuff.||||||
25716|Edeowie Limestone Member|62784|5|Briefly described|p8 Fig.1|Cambrian|Cambrian|Arrowie Basin. Basal member of Billy Creek Formation. Overlies Oraparinna Shale unit of Hawker Group.||||||20-MAR-12
25716|Edeowie Limestone Member|63569|5|Briefly described|p118-120|Cambrian|Cambrian|||Unit in Billy Creek Formation.||Overlies Oraparinna Shale unconformably, at least locally.||
25716|Edeowie Limestone Member|65686|5|Briefly described|p409 Fig 2|Early Cambrian|Early Cambrian|||Of Billy Creek Formation.||Overlies the Coads Hill Member.||07-MAY-12
25716|Edeowie Limestone Member|65892|5|Briefly described|p7 Fig.3, p28.|Early Cambrian|Early Cambrian|Arrowie Basin. 7m thick. A useful marker horizon. ||Unit in Billy Creek Formation.||Is overlain by Warragee Member of Billy Creek Formation.|Planar to wavy laminated cryptalgal dolomitic mudstone.|
25716|Edeowie Limestone Member|65925|5|Briefly described|p14 Fig.2.2, Appendix 2.||||||||Dolomitic mudstone with planar to wavy lamination; peloidal sandy limestone with tuff beds.|
25716|Edeowie Limestone Member|68735|5|Briefly described|p234|||~ 7 m thick. Regarded as either the top Member of the Oraparinna Shale (Moore 1979) or as the bottom Member of the Billy Creek Formation.||||Underlain by the Oraparinna Shale.|Comprises cryptomicrobial laminated flaggy dolomite.|10-APR-17
25716|Edeowie Limestone Member|70835|6|Mentioned|p335|Cambrian|Cambrian|Arrowie Basin, Flinders Ranges. See also references to Edeowie Limestone on p336-337.||Billy Creek Formation.||Overlies Oraparinna Shale. Is overlain by Billy Creek Formation.||
25716|Edeowie Limestone Member|72429|6|Mentioned|p972|||Occurs at Ten Mile Creek, near Wilkawillina Gorge. 7m thick. Also written as Edeowie Limestone.||||Overlies the Oraparinna Shale. Potentially equivalent to the Brillig Catch Member.|Microbial laminites and dolomitic mudstones.|
81701|El Alamein Kimberlite|71129|5|Briefly described|p136|Early Jurassic|Early Jurassic|Geological Province: Gawler Craton. Dating of rutile yielded age of c. 190 Ma; zircons yielded age of c. 178 Ma, which more likely reflect age of intrusion.|c. 178 Ma|||||
25895|Emeroo Subgroup|22631|6|Mentioned|p177|Cryogenian|Cryogenian|||||||
25895|Emeroo Subgroup|22772|5|Briefly described|Table13.1|Cryogenian|Cryogenian|||||||
25895|Emeroo Subgroup|22857|5|Briefly described|Tb. 13.1 (insert p70-71)|Torrensian|Torrensian|Of the Burra Group.||||||
25895|Emeroo Subgroup|22869|5|Briefly described|P37, P38, Table2|||||||||
25895|Emeroo Subgroup|22889|4|Described|p31-34 & p37|Adelaidean|Adelaidean|Of the Burra Group.  Age - Torrensian.  The upper boundary of the Emeroo Subgroup is revised.||||||11-SEP-07
25895|Emeroo Subgroup|23054|6|Mentioned|p11|||||||||
25895|Emeroo Subgroup|23719|4|Described|p25|Neoproterozoic|Neoproterozoic|Formerly Emeroo Quartzite. See also page 25 table 7. Of Burra Group. Overlain by Umberatana Group. Underlain by Callanna Group. Geological Province: Gawler Craton. Max. thickness >300 m.||||||11-SEP-07
25895|Emeroo Subgroup|24175|3|Fully described|p10-11|Neoproterozoic|Neoproterozoic|Of Burra Group.  Max. exposed thickness: 3920m.||||||
25895|Emeroo Subgroup|24321|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Burra Group.||||||11-SEP-07
25895|Emeroo Subgroup|24546|5|Briefly described|p2 - 3 Fig.2|Neoproterozoic|Neoproterozoic|Of Burra Group. Geological Province: Adelaide Fold Belt.||||||16-JAN-08
25895|Emeroo Subgroup|37854|2|Defined|p13|Adelaidean|Adelaidean|Torrensian||||||
25895|Emeroo Subgroup|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Torrensian||||||
25895|Emeroo Subgroup|39490|6|Mentioned|Fig.1(6)|||||||||
25895|Emeroo Subgroup|40294|6|Mentioned|p41|||See also Table 2||||||
25895|Emeroo Subgroup|41256|5|Briefly described|p7|||||||||
25895|Emeroo Subgroup|41401|6|Mentioned|Table 4|||||||||
25895|Emeroo Subgroup|41402|6|Mentioned|p41|||||||||
25895|Emeroo Subgroup|41403|6|Mentioned|p54|||||||||
25895|Emeroo Subgroup|41404|4|Described|p89|||||||||
25895|Emeroo Subgroup|41405|6|Mentioned|Fig.55|||||||||
25895|Emeroo Subgroup|41526|6|Mentioned|p47|||||||||
25895|Emeroo Subgroup|42098|6|Mentioned|Table 2 P54|||||||||
25895|Emeroo Subgroup|42222|4|Described|p12|||||||||
25895|Emeroo Subgroup|42235|4|Described|p134|||See also Fig.3||||||
25895|Emeroo Subgroup|42237|5|Briefly described|p87|||See also Fig.2||||||
25895|Emeroo Subgroup|42238|5|Briefly described|p72|||||||||
25895|Emeroo Subgroup|42506|5|Briefly described|Map legend|Adelaidean (Torrensian)||||||||
25895|Emeroo Subgroup|42813|4|Described|p16|||Of the Burra Group.||||||11-SEP-07
25895|Emeroo Subgroup|43052|4|Described|p177|||Of the of Burra Group.||||||11-SEP-07
25895|Emeroo Subgroup|43053|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Fluviodeltaic sandstone, conglomerate, siltstone and minor dolomite.||||||26-MAY-05
25895|Emeroo Subgroup|43258|5|Briefly described|Map Legend||Neoproterozoic|||||||
25895|Emeroo Subgroup|43298|5|Briefly described|Map Legend||Adelaidean|||||||
25895|Emeroo Subgroup|60718|5|Briefly described|p49 Fig. 2, p52|Adelaidean|Adelaidean|Max. exposed thickness: ~4000m. Geological Province: Adelaide Geosyncline.||Of Burra Group.|Includes Witchelina Quartzite, Willawalpa Formation and Top Mount Sandstone Beds.|||15-APR-11
25895|Emeroo Subgroup|60953|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Fluviodeltaic sandstone, conglomerate, siltstone, minor dolomite.||||||
25895|Emeroo Subgroup|60959|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Of the Burra Group.||||||
25895|Emeroo Subgroup|61108|5|Briefly described|map legend|Adelaidean|Adelaidean|Fluviodeltaic sandstone, conglomerate, siltstone and minor dolomite.||||||
25895|Emeroo Subgroup|62592|5|Briefly described|p50 Table 5.1, p57.|Sturtian|Torrensian|Adelaide Geosyncline.||Basal unit in Burra Group.||Is overlain by Mundallio Subgroup.|Fluvial arkose, siltstone, dolomite.|
25895|Emeroo Subgroup|62664|5|Briefly described|p138 Fig.2.|Neoproterozoic|Neoproterozoic|||Unit in lower Burra Group.|||Sandstone, quartzite, conglomerate.|
25895|Emeroo Subgroup|62724|5|Briefly described|p17 Fig. 4|Torrensian|Torrensian|Of the Burra Group.||||||07-FEB-11
25895|Emeroo Subgroup|63020|5|Briefly described|p974 Fig. 2|||Of the Burra Group. ||||||
25895|Emeroo Subgroup|63489|5|Briefly described|Map legend|Adelaidean|Adelaidean|Sandstone, in part with heavy mineral laminations; conglomerate, siltstone and minor carbonate.||||||10-SEP-07
25895|Emeroo Subgroup|64647|6|Mentioned|p38 Fig. 1|||Includes Alddate Sandstone.||||||
25895|Emeroo Subgroup|64793|6|Mentioned|p284 fig 3, p290|||Adelaide Rift Complex.||Burra Group.||||
25895|Emeroo Subgroup|64796|6|Mentioned|p191 Fig.9|Neoproterozoic|Neoproterozoic||||Includes Rhynie Sandstone and Murrana Beds.|||
25895|Emeroo Subgroup|64797|6|Mentioned|p153 Fig.2|Cryogenian|Cryogenian|Adelaide Rift Complex. Lithology/rank not shown on diagram.||||||
25895|Emeroo Subgroup|65375|6|Mentioned|p25.|||||Unit in Burra Group.|Includes Rhynie Sandstone.|||
25895|Emeroo Subgroup|65376|6|Mentioned|p229 Fig.6.39.|Neoproterozoic|Neoproterozoic|||||||
25895|Emeroo Subgroup|66884|5|Briefly described|p38, p39 Fig.2, p41 Fig.3|||||Burra Group|Witchelina Quartzite, Willawalpa Formation, Top Mount Sandstone beds.|Is conformably overlain by Camel Flat Shale Member.|Sand-dominated.|14-DEC-16
25895|Emeroo Subgroup|67870|5|Briefly described|p9|Neoproterozoic|Neoproterozoic|Adelaide Rift System.||Burra Group.||||
25895|Emeroo Subgroup|69019|4|Described|p38-39.|Neoproterozoic|Neoproterozoic|Of Forbes et al. (1981); redefined by Preiss and Cowley (1999).||Unit in Burra Group.|Includes Top Mount Sandstone Beds, Willawalpa Formation and Witchelina Quartzite.||Predominantly quartz-rich succession.|
25895|Emeroo Subgroup|70384|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Adelaide Geosyncline.  Age shown more specifically as Torrensian [Cryogenian].||Burra Group.|Includes Humanity Seat, Opaminda Formations; Woodnamoka Phyllite; Blue Mine Conglomerate; Wortupa Quartzite.|Is overlain by Mundallio Subgroup.||18-JAN-19
25895|Emeroo Subgroup|70405|6|Mentioned|p50,p51 table 4|Neoproterozoic|Neoproterozoic||||Includes Bungaree Quartzite, River Wakefield Formation, Rhynie Sandstone||Siliciclastic metasediments.|
25895|Emeroo Subgroup|70819|5|Briefly described|p11, 13, 18-19|Neoproterozoic|Neoproterozoic|Western Clare Valley. Fluvial to shallow-marine environments.|c.800 Ma.|Burra Group.|Rhynie Sandstone, Blyth Dolomite, River Wakefield Formation, Bungaree Quartzite.|Overlies Callanna Group. Is overlain by Mundallio Subgroup.|Sandstones, siltstones, shales, dolomites, and minor basalt.|
25895|Emeroo Subgroup|71348|6|Mentioned|p202|||Geological province: Gawler Craton.||||||
25895|Emeroo Subgroup|73093|5|Briefly described|map legend|Neoproterozoic|Neoproterozoic||||||Quartzite, sandstone, dolomite, conglomerate.|09-DEC-21
25895|Emeroo Subgroup|73103|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic||||||Quartzite, sandstone, dolomite, conglomerate.|
25895|Emeroo Subgroup|73188|5|Briefly described|p316|Neoproterozoic|Neoproterozoic|Mount Lofty Ranges.||Burra Group|Aldgate Sandstone|||
25895|Emeroo Subgroup|74367|5|Briefly described|p7 Fig.6, p8-9, p12-14, p18, p20|Tonian|Tonian|See also Emeroo subgroup p9. Minimum age constrained to ca. 790 Ma by the Kooringa Member.||Burra Group|Boucaut Volcanics, Rhynie Sandstone, Humanity Seat Formation, Blyth Dolomite, Blue Mine Conglomerate, River Wakefield Formation|||
81765|Engenina Granite|67323|5|Briefly described|p33|||Northern Gawler Craton. Syn-tectonic with the waning stages (~1725-1690 Ma) of the Kimban Orogeny.|~1690 Ma.|||||
81765|Engenina Granite|72459|6|Mentioned|p51|Palaeoproterozoic|Palaeoproterozoic||1691 +/- 25 Ma|||||
27399|Enorama Shale|22510|5|Briefly described|p39, table1|||Redefined by Dyson(1997), to include upper part of old Etina Formation.||||||
27399|Enorama Shale|22631|6|Mentioned|p178|||Age: Marinoan||||||05-JUL-13
27399|Enorama Shale|23211|6|Mentioned|p45|||Interpreted to be of deep water origin in Umberatana and Wilpena Groups.||||||
27399|Enorama Shale|23250|5|Briefly described|p1124 Fig.2||Cryogenian|Of Umberatana Group. Correlate of Wilmington Formation equivalent.||||||30-SEP-08
27399|Enorama Shale|23394|5|Briefly described|Map legend|Proterozoic|Proterozoic|||||||
27399|Enorama Shale|23818|4|Described|p64 Fig.22, p68, 69|Neoproterozoic|Neoproterozoic|Uppermost unit of the Farina Sub-Group. Underlying unit: Tarcowie Siltstone. Max. thickness: 1500 ft. Well laminated.||||||
27399|Enorama Shale|23913|4|Described|p110 Fig. 2|Adelaidean|Adelaidean|Geological province: Central Flinders Zone. Of the Umberatana Group.  Underlying Unit: Etina Formation.  Overlying Unit: Trezona Formation.||||||
27399|Enorama Shale|24175|5|Briefly described|p13|Neoproterozoic III|Neoproterozoic|Of the Umberatana Group.   Max. thickness: 105m.||||||
27399|Enorama Shale|24176|4|Described|p13, p24 Tb. 1|Adelaidean|Adelaidean|Of the Farina Sub-Group.  Silty dolomitic shales.  Overlies Willochra Sub-Group.  Partly equivalent to Amberoona Formation.  Max. thickness: 150m. Age is Marinoan.  Geological Province: Mount Painter Province.||||||
27399|Enorama Shale|24321|5|Briefly described|Map legend|Adelaidean|Adelaidean|||||||
27399|Enorama Shale|24476|4|Described|p547 Fig. 4|Vendian|Vendian|Overlies the Etina Formation. Overlain by the Trezona Formation.  Geological Province: Adelaide fold belt.||||||
27399|Enorama Shale|29778|6|Mentioned|p167|||||||||
27399|Enorama Shale|29780|5|Briefly described|p40|||||||||
27399|Enorama Shale|29834|6|Mentioned|p198|||||||||
27399|Enorama Shale|30176|6|Mentioned|Map legend|Adelaidean|Adelaidean|Marinoan||||||
27399|Enorama Shale|30177|5|Briefly described|p82|||||||||
27399|Enorama Shale|30198|6|Mentioned|p96|||See also Table 2 - aquifers and lithology||||||
27399|Enorama Shale|30801|6|Mentioned|p5|||Marinoan. Table P5-6||||||
27399|Enorama Shale|30802|4|Described|Table 1|||Marinoan age||||||
27399|Enorama Shale|30807|6|Mentioned|p103|||Suggested map symbol||||||
27399|Enorama Shale|32146|6|Mentioned|Fig.3|||||||||
27399|Enorama Shale|32505|6|Mentioned|Table 3|||||||||
27399|Enorama Shale|32510|6|Mentioned|Fig.1|||||||||
27399|Enorama Shale|32720|6|Mentioned|Table 1|||||||||
27399|Enorama Shale|32722|6|Mentioned|Fig.3|||Adelaidean. Stromatolite||||||
27399|Enorama Shale|32724|6|Mentioned|p520|||Marinoan. Lithology||||||
27399|Enorama Shale|33474|6|Mentioned|Fig.2|||||||||
27399|Enorama Shale|34267|6|Mentioned|Fig.|||The Oraparinna & Enorama diapiric structures.||||||
27399|Enorama Shale|34291|6|Mentioned|p13|||See also P73. Adelaidean||||||
27399|Enorama Shale|34534|6|Mentioned|Fig.2.13|||||||||
27399|Enorama Shale|34535|5|Briefly described|p68|||||||||
27399|Enorama Shale|35075|6|Mentioned|p77|||||||||
27399|Enorama Shale|35255|6|Mentioned|Fig.7|||||||||
27399|Enorama Shale|35582|6|Mentioned|p51|||||||||
27399|Enorama Shale|36245|6|Mentioned|p5|||||||||
27399|Enorama Shale|36733|6|Mentioned|Table 5|||||||||
27399|Enorama Shale|37015|6|Mentioned|Fig.2|||||||||
27399|Enorama Shale|37461|4|Described|p341|||See also Table 5.I.||||||12-SEP-18
27399|Enorama Shale|37627|6|Mentioned|Fig.2|||||||||
27399|Enorama Shale|38110|6|Mentioned|p3|||||||||
27399|Enorama Shale|38157|6|Mentioned|Table IV|||||||||
27399|Enorama Shale|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Marinoan||||||
27399|Enorama Shale|40852|6|Mentioned|Fig.3.2|||||||||
27399|Enorama Shale|40910|6|Mentioned|p12|||||||||
27399|Enorama Shale|40911|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
27399|Enorama Shale|41405|3|Fully described|p176|||See also p161 and p203.||||||12-SEP-18
27399|Enorama Shale|41500|6|Mentioned|Fig.1|||||||||
27399|Enorama Shale|41526|6|Mentioned|p5|||||||||
27399|Enorama Shale|42098|5|Briefly described|p54|||||||||
27399|Enorama Shale|42109|6|Mentioned|Fig.1 P19|||||||||
27399|Enorama Shale|42222|6|Mentioned|p17|||||||||
27399|Enorama Shale|42238|6|Mentioned|p77|||||||||
27399|Enorama Shale|42239|6|Mentioned|p150|||||||||
27399|Enorama Shale|42720|5|Briefly described|map legend|Marinoan||||||||
27399|Enorama Shale|42813|5|Briefly described|p20|||of Farina Subgroup||||||
27399|Enorama Shale|42882|5|Briefly described|Fig.7 P12, Table1 P3|||Of Umberatana Group.||||||30-SEP-08
27399|Enorama Shale|43052|5|Briefly described|p189,Table 6.1|||||||||
27399|Enorama Shale|43845|5|Briefly described|Fig3 p43||Neoproterozoic|In Umberatana Group||||||12-JUL-16
27399|Enorama Shale|44659|5|Briefly described|map legend|||Marinoan, lithology.||||||
27399|Enorama Shale|46865|6|Mentioned|Table 2|||||||||
27399|Enorama Shale|60955|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Of the Amberoona Formation.||||||
27399|Enorama Shale|60959|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Of the Upalinna Subgroup. Laminated grey-green and minor red shale, silty shale and rare fine grained sandstone.||||||
27399|Enorama Shale|61236|6|Mentioned|p24 Fig. 1|Adelaidean|Adelaidean|||||||
27399|Enorama Shale|61732|5|Briefly described|p28 Fig. 13|Marinoan|Marinoan|Of the Upalinna Subgroup (Umberatana Group). Includes the Wundowie Limestone Member. Geological Province: Adelaide Rift Complex.||||||07-FEB-11
27399|Enorama Shale|62085|6|Mentioned|p20 fig 5|Cryogenian|Cryogenian|||Umberatana Group||||
27399|Enorama Shale|62592|5|Briefly described|p50 Table 5.1.|Marinoan|Marinoan|Adelaide Geosyncline.||Unit in Upalinna Subgroup.||Overlies Etina Formation. Is overlain by Trezona Formation.|Fine siltstone.|
27399|Enorama Shale|62903|6|Mentioned|p729|||interglacial. Date from Enorama Shale and Trezona Formation|690+/-21 Ma Rb-Sr whole-rock shale date, imprecise|||||
27399|Enorama Shale|64797|6|Mentioned|p153 Fig.2, p164 Fig.11, p169 Fig.12|Ediacaran|Ediacaran|Adelaide Rift Complex. Lithology/rank not shown on diagram.||||||
27399|Enorama Shale|64801|6|Mentioned|p109, p110 Fig.2, p111-116, p119|Cryogenian|Cryogenian|Dalgarno and Johnson (1966). Redefined by Preiss et al. (1998). Includes a reef complex against the Enorama Diapir (described in detail).||Umberatana Group.|Wundowie Limestone Member.|||
27399|Enorama Shale|64846|5|Briefly described|p197-200 Figs.2-5, p202 Tb.1  |Cryogenian|Cryogenian|See also p205-206 Tb.2, p211. Carbon isotope details.||Of the Upalinna Subgroup.|Includes Wundowie Limestone Member.|||
27399|Enorama Shale|65493|5|Briefly described|p917, 924, Fig 1,2,4,12,14|Cryogenian|Cryogenian|Of Upalinna Subgroup. Includes Wundowie Limestone Member. Gradational contact with underlying Amberoona Formation. Unconformably overlain by Elatina Formation. Shale with 3 basin-wide stromatolite horizons near base.||||||
27399|Enorama Shale|65892|5|Briefly described|p33 Fig.18, p39. |Cryogenian|Cryogenian||c.640 Ma.|Unit in Umberatana Group.||Overlies Etina Formation. Is overlain by Trezona Formation.|Grey-green shale.|
27399|Enorama Shale|65925|5|Briefly described|Appendix 2.||||||||Shale, grey-green and minor red, laminated; silty shale, rare fine grained sandstone.|
27399|Enorama Shale|67030|5|Briefly described|p408, p409 Fig. 2|Cryogenian|Cryogenian|Shown as partial lateral equivalent to Wilmington Formation. Diagenetic age for authigenic monazite from sandstone from the Enorama Shale.|680 +/- 23 Ma (Th-U-total Pb, Mahan et al. 2010)|Farina Subgroup||Overlies the Waukaringa Siltstone, underlies the Gumbowie Arkose of Yerelina Subgroup.||26-APR-12
27399|Enorama Shale|67180|4|Described|p600, p606-607; Figs. 1, 2, 4, 7, 10|Cryogenian|Cryogenian|Marinoan age. Defined by Dalgarno and Johnson in Thompson et al. 1964. Defining feature of 3 thin distinct stromatolitic limestone beds of the Wundowie Limestone Member towards base. Above this is a fine-grained shale. Th-U-total Pb age from authigenic monazite grains is inconsistent with Kendall et al. (2006) and Fanning and Link (2008). |680 +/- 23 Ma Th-U-total Pb (Mahan et al. 2010)|Unit in Upalinna Subgroup|Includes Wundowie Limestone Member|Conformably overlies the Amberoona Formation; unconformably overlain by the Elatina Formation.|Green and grey shales, calcareous silty shale, stromatolitic dolomite.|12-SEP-18
27399|Enorama Shale|67979|4|Described|p536, p529, p530, p531, p534, p541-543|Marinoan||In the Central and Northern Flinders Ranges, the base is defined by Wundowie Limestone Member. Above this member this unit occurs as thick, monotonous, very fine-grained calcareous shales indicating return to deeper marine conditions. See Figs.1, 2 and 5.||Upalinna Subgroup|Wundowie Limestone Member|Conformably overlies Amberoona Formation; unconformably overlies Etina Formation.|Fine-grained calcareous shales hosting sandy and stromatolitic limestones.|22-SEP-14
27399|Enorama Shale|68241|6|Mentioned|p22-23 Fig.2|||||||Overlain by the Elatina Formation.||
27399|Enorama Shale|70021|6|Mentioned|p97|Neoproterozoic|Neoproterozoic|Northern Flinders Ranges, Adelaide Geosyncline.||||||
27399|Enorama Shale|70031|4|Described|p245-246|Cryogenian|Cryogenian|Adelaide Geosyncline. Upper interglacial, transgressive succession. Thickness: 140m. Sandstone from Enorama Shale yeild diagenetic Th-U-total Pb age of 680+\-23 Ma for authigenic monazite (Mahan et al., 2010).||Unit of Upalinna Subgroup.||Overlain by Trezona Formation. Underlain by Etina Formation.|Green shale.|
27399|Enorama Shale|70082|6|Mentioned|p2-3|Cryogenian|Cryogenian|Flinders Ranges. Authigenic monazite cement in the sandstone of the Enorama Formation dated using Th-U-Pb at 680+\-23 Ma (Mahan et al., 2010).||||||
27399|Enorama Shale|70384|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Adelaide Geosyncline. Age shown more specifically as Marinoan [Cryogenian].||Of Upalinna Subgroup.|Includes Wundowie Limestone Member.||Grey-green and minor red, laminated shale; silty shale; rare fine-grained sandstone.|23-JAN-19
27399|Enorama Shale|70407|5|Briefly described|p103 Fig 2, p113|Neoproterozoic|Neoproterozoic|Age: Marinoan.||Of Umberatana Group.|Includes Artipena Dolomite Member.|||
27399|Enorama Shale|70744|6|Mentioned|p939-940|||New authigenic monazite ages (earliest at 680 +/- 23 Ma) indicate that the Sturtian glaciation was no younger than 690 Ma and possibly older.||||||
27399|Enorama Shale|71237|14|Not recorded|p10, 12, 17|||||||||
27399|Enorama Shale|72449|5|Briefly described|p1, p2 Map Legend|Neoproterozoic|Neoproterozoic|Quieter, deeper marine environment than underlying Etina Formation.||||Overlies Etina Formation and underlies Trezona Formation.|Laminated grey-green and minor red shale, silty shale and rare fine-grained sandstone.|
27399|Enorama Shale|72473|6|Mentioned|p4|||||||||
27399|Enorama Shale|72601|6|Mentioned|p11, p19|Cryogenian|Cryogenian|Adelaide Rift Complex.||Umberatana Group|Wundowie Limestone Member|||
27399|Enorama Shale|72613|6|Mentioned|p2 fig 1, p3|Cryogenian|Cryogenian |Shown as Marinoan age. Northern Flinders Ranges.||Umberatana Group||||
27399|Enorama Shale|74367|5|Briefly described|p7 Fig.6, p8, p11, p19|Cryogenian|Cryogenian|Geochronology is from electron microprobe of authigenic monazite (Mahan et al., 2010), is a minimum depositional age not considered accurate based on stratigraphic relation to Tindelpina Shale Member and Wilyerpa Formation.|680+/-23 Ma Th-U-total Pb age|Upalinna Subgroup||||
27149|Eregunda Sandstone Member|35835|2|Defined|p207|Middle Cambrian|Early Cambrian|Lower to Middle Cambrian||||||
27149|Eregunda Sandstone Member|35954|4|Described|p1229|||Sedimentary aspects discussed throughout article.||||||
27149|Eregunda Sandstone Member|36495|6|Mentioned|p127|||||||||
27149|Eregunda Sandstone Member|37326|6|Mentioned|p3|||||||||
27149|Eregunda Sandstone Member|37802|6|Mentioned|Fig.2|||||||||
27149|Eregunda Sandstone Member|38771|6|Mentioned|p56|||||||||
27149|Eregunda Sandstone Member|42090|6|Mentioned|p26|||||||||
27149|Eregunda Sandstone Member|42269|6|Mentioned|p335|||||||||
27149|Eregunda Sandstone Member|44133|5|Briefly described|p27|||Of the Billy Creek Formation. Maximum Thickness: 166m. ||||||
27149|Eregunda Sandstone Member|60418|5|Briefly described|p134 Fig.1|||Of Billy Creek Formation||||||
27149|Eregunda Sandstone Member|60959|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of the Billy Creek Formation. Greyish-red arkose with minor interbedded shale and siltstone.||||||
27149|Eregunda Sandstone Member|62784|5|Briefly described|p8 Fig.1|Cambrian|Cambrian|Arrowie Basin. Top of Billy Creek Formation.||||||
27149|Eregunda Sandstone Member|63569|5|Briefly described|p118-119|Cambrian|Cambrian|||Unit in Billy Creek Formation.||||
27149|Eregunda Sandstone Member|65892|5|Briefly described|p41-42.  |Early Cambrian|Early Cambrian|Thin-bedded; ripple marks, arthropod tracks and halite casts common.||Topmost unit in Billy Creek Formation.||Is overlain conformably by Aroona Creek Limestone.|Fine- to medium-grained, red, micaceous feldspathic sandstone.|
27149|Eregunda Sandstone Member|66589|6|Mentioned|p178|Middle Cambrian|Middle Cambrian|Case studies cited; not visited in the field by the authors of this study.||||||
27149|Eregunda Sandstone Member|70835|6|Mentioned|p335|Cambrian|Cambrian|Arrowie Basin, Flinders Ranges. See also reference to Edeowie Limestone Member on p335.||Billy Creek Formation.||||
23582|Erudina Siltstone Member|23981|5|Briefly described|p54|||Of the Billy Creek Formation. Contains red and green sandstones and siltstones within predominantly green, calcareous, micaceous mudstones, which are generally flat or lenticular bedded.||||||
23582|Erudina Siltstone Member|36495|2|Defined|p124|Early Cambrian|Early Cambrian|||||||
23582|Erudina Siltstone Member|37802|4|Described|p71|||||||||
23582|Erudina Siltstone Member|38108|6|Mentioned|Table 1|||||||||
23582|Erudina Siltstone Member|42269|6|Mentioned|p336|||||||||
23582|Erudina Siltstone Member|44133|4|Described|p27|||Of the Billy Creek Formation. Conformably overlies part of the Coads Hill Member. Correlates with Warragee Member. Maximum Thickness: 270m.||||||
23582|Erudina Siltstone Member|60889|5|Briefly described|p247 Fig.4|Early Cambrian|Early Cambrian|||Billy Creek Formation||||
23582|Erudina Siltstone Member|65925|6|Mentioned|p14 Fig.2.2.|Early Cambrian|Early Cambrian|||||||
23582|Erudina Siltstone Member|68735|6|Mentioned|p238|||||Of the Billy Creek Formation.||||
35883|Ethiudna Subgroup|23347|2|Defined|p51 Tb. 1, p53|Statherian|Statherian|Of Curnamona Gp (Willyama Supergp). Formerly "Ethiudna calc-silicate group" of Campana (1953) and former  "Bimba formation". Overlies Wiperaminga Subgp. Age: ~1.71Ga. Abminga Subsuite occurs in lower part. Variable lithology - details included.||||||24-MAR-09
35883|Ethiudna Subgroup|23476|5|Briefly described|p50|||Of Curnamona Group.||||||
35883|Ethiudna Subgroup|24289|5|Briefly described|p46|Paleoproterozoic|Paleoproterozoic|Of Curnamona Group.||||||07-NOV-08
35883|Ethiudna Subgroup|24431|5|Briefly described|p189 Fig. 1|||Of the Curnamona Group. Overlies the Wiperaminga Subgroup. Overlain by the Bimba Formation. Geological Province: Olary Domain.||||||
35883|Ethiudna Subgroup|60485|5|Briefly described|p28 Fig. 2, p30|||Of the Curnamona Group. Quartz-feldspar-biotite composite gneiss. Geological Province: Olary Domain.||||||22-OCT-08
35883|Ethiudna Subgroup|61734|5|Briefly described|p52 Fig.2|Statherian|Statherian||1.71 Ga|Of the Curnamona Group||Overlies Wiperaminga Subgroup. Is intruded by Basso and Lady Louise Suites. Is overlain by Bimba Formation.|Calcic minerals, stratiform iron sulphide layers.|
35883|Ethiudna Subgroup|61736|5|Briefly described|p666 Fig. 3|Paleoproterozoic|Paleoproterozoic|Of Curnamona Group. Includes Peryhumuck Formation and Whey Whey Formation. Geological province: Olary Domain.||||||24-FEB-10
35883|Ethiudna Subgroup|62373|5|Briefly described|p503|Paleoproterozoic|Paleoproterozoic|Of the Curamona Group (Willyama Subgroup). Well-bedded, pelitic sediments with calc-silicate rocks. Intercalated with rocks of the Montstephan Metabasalt. Geological Province: Curnamona Province/Olary Domain.||||||07-NOV-08
35883|Ethiudna Subgroup|62514|5|Briefly described|p748 Fig. 3|Mesoproterozoic|Mesoproterozoic|Of the Curnamona Group. Age: <1700Ma. Geological Province: Olary Domain/Curnamona Province||||||16-SEP-09
35883|Ethiudna Subgroup|62535|4|Described|p666, p670, p672|Paleoproterozoic|Paleoproterozoic|Exploration target for strata-bound epigenetic Cu-Au-Mo mineralization. Also appears as Ethiuda Subgroup on p666, p670, p671.|c.1710 Ma.|Curnamona Group.|Peryhumuck, Whey Whey Formations.|Overlies Wiperaminga Subgroup. Interbedded with Basso Suite.|Fine-grained albitized sediments with a variable calc-silicate component. Includes volcanic units.|
35883|Ethiudna Subgroup|62592|5|Briefly described|p14, p16 Fig.2.2.|||Olary Domain, Curnamona Province.||Upper unit in Curnamona Group.||Is intruded by Basso Suite and Woman-in-White Amphibolite.|Calcareous and evaporitic.|
35883|Ethiudna Subgroup|62993|4|Described|p2-p4, 6-8, 10,12,14,16, 20, 37-40, 42,|Paleoproterozoic|Paleoproterozoic|Olary Domain.|~1715 Ma|Curnamona Group|Includes Peryhumuck Formation, Cathedral Rock Formation, Whey Whey Formation, Waukaloo Formation, Toraminga Formation, Bewooloo Formation|Overlies Tommie Wattie Formation, George Mine Formation.Overlain by Larry Macs, Raven Hill Subgroups.|Siliceous psammopelite, epidotitic amphibole albitites, laminated calcalbitite, manganiferous albitite.|19-DEC-21
35883|Ethiudna Subgroup|63102|4|Described|p10,13-22,26-29,30,34-35,37,39-41,44,49|Statherian|Statherian|Geological province: Olary Domain, Curnamona Province. Relatively thin sequence with evidence of evaporitic deposition in the Curnamona Province. Characterised by variable carbonate/calc-silicate, pyrite and fine-grained albitic-psammite lithologies. Hosts significant Cu-Au mineralisation, preferentially occuring at the contact between Ethiudna and Wiperaminga subgroups. See p27-29 for descriptions on unnamed lithological units. Contains stratiform mineralisation; small BIFs and Mc silicates. Also shows stratabound mineralisation; disseminated sediment-hosted Fe, Cu, Zn, Co, W, U, F. See also p53-54,57-60.||Unit of Curnamona Group.|Includes Bimba, Peryhumuck and Whey-Whey formations.|Underlain by Wiperaminga Subgroup. Intruded by Billeroo alkanline magmatic complex. Overlies the George Mine Formation.||22-OCT-19
35883|Ethiudna Subgroup|63186|5|Briefly described|p66, p67|Paleoproterozoic|Paleoproterozoic|Of the Curnamona Group (Willyama  Supergroup). Calc-silicate rocks - dominate in the Olary Domain of the Curnamona Province. Intruded by Rasp Ridge and Hores Gneisses.||||||07-NOV-08
35883|Ethiudna Subgroup|63539|5|Briefly described|p33|||Geological Province: Olary Domain/Curnamona Province. Intruded by the Billeroo alkaline magmatic complex.||||||07-FEB-08
35883|Ethiudna Subgroup|63866|5|Briefly described|p40|||Olary Domain, Curnamona Province.||Curnamona Group||Overlies the Wiperaminga Subgroup. Unconformably overlain by the Saltbush Group.||
35883|Ethiudna Subgroup|64097|5|Briefly described|p322|||Contains layered albitic metsediments.||||||07-FEB-11
35883|Ethiudna Subgroup|64741|4|Described|p301 Fig. 4|Paleoproterozoic|Paleoproterozoic|Of Curnamona Gp. Includes Cathedral Rock, Bewooloo, Peryhumuck, Waukaloo, Whey Whey + Toraminga Fm. Geol.prov: Olary Domain.Overlies Wiperaminga Subgp. Max. thickness: 400m. Tommie Wattie Formation included in this subgroup by Flint (2001). Brecciation||||||07-FEB-11
35883|Ethiudna Subgroup|64742|5|Briefly described|p321 Fig.3, pp325-326.|||Major and trace element analyses, and Sm-Nd isotope data, are detailed.||Unit in Curnamona Group.||Overlies Wiperaminga Subgroup.|Quartz-plagioclase-mica schist, quartzite, calc-albitite.|29-MAR-12
35883|Ethiudna Subgroup|64744|5|Briefly described|p353 Fig.4, p354. |Statherian|Statherian|Olary Domain.||Unit in Willyama Supergroup.||Overlies Wiperaminga Subgroup.|Psammopelitic schists and gneisses.|04-FEB-16
35883|Ethiudna Subgroup|64944|4|Described|p27, p28 Fig. 1, p29 Tb.1|Paleoproterozoic|Paleoproterozoic|Upper part of Curnamona Group.Contains Bewooloo, Cathedral Rock, Peryhumuck, Waukaloo, Whey Whey and Topraminga Fms. Overlies Wiperaminga Subgroup. Age: ~1711.5-1708Ma. Generally equivalent to the "Calcsilicate Suite" of Clarke et al (1986). Base varies.||||||07-FEB-11
35883|Ethiudna Subgroup|65407|6|Mentioned|p239 Fig.3|||||Curnamona Group.|"Bimba Formation".|||
35883|Ethiudna Subgroup|66302|5|Briefly described|p36 Fig.9, p37, p39|Statherian|Statherian|Olary Domain, Curnamona Province. |||Includes the Toraminga Formation, Whey Whey Formation, Bewooloo Formation, Cathedral Rock Formation, Peryhumuck Formation and the Waukaloo Formation.|Overlies the Wiperaminga Subgroup. Unconformably overlain by the Saltbush Group.||
35883|Ethiudna Subgroup|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Olary Domain.|1712 +/- 2 Ma.|Curnamona Group.||||
35883|Ethiudna Subgroup|67540|5|Briefly described|p29 Tb.2|||||Of the Willyama Supergroup.||Intruded by the Billeroo Intrusive Complex.||04-FEB-16
35883|Ethiudna Subgroup|68126|5|Briefly described|p29|Paleoproterozoic|Paleoproterozoic|Olary Domain, Curnamona Province.||Curnamona Group.||||
35883|Ethiudna Subgroup|69213|6|Mentioned|p34|Paleoproterozoic|Paleoproterozoic|Olary Domain, Curnamona Province.||?Curnamona Group||Wiperaminga Subgroup underlies.|Migmatites.|
35883|Ethiudna Subgroup|69650|5|Briefly described|p6, p36|||||Unit in Willyama Supergroup.||Intruded by Billeroo Intrusive Complex.||04-FEB-16
35883|Ethiudna Subgroup|70339|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|||Willyama Supergroup.|Cathedral Rock, Peryhumuck Formations.||Metasediments and local volcanic rocks; characterised by calc-silicate minerals and alkali feldspar. Generally magnetite- or haematite-bearing. Local pseudomorphs of diagenetic or evaporitic minerals.|02-FEB-16
35883|Ethiudna Subgroup|70340|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|||Probably includes Peryhumuck Formation.|||Metasediments and local volcanic rocks; characterised by calc-silicate minerals and alkali feldspar. Generally magnetite- or haematite-bearing. Local pseudomorphs of diagenetic or evaporitic minerals.|
35883|Ethiudna Subgroup|70405|4|Described|p9 table 1, p15, p18,p38, p43 Table 3, |Paleoproterozoic|Paleoproterozoic|Bedding is well preserved except in pelitic lithologies and poorly bedded schistose psammites. Some units are highly magnetic. Carbonate rhombs cut laminations in feldspathic psammites.Felsic volcanics are commonly intercalations as opposed to lava flows.|1710 Ma-1720 Ma|Curnamona Group|Includes Tommie Wattie Formation, Toraminga Formation, Cathedral Rock Formation, Peryhumuck Formation.|Underlies Bimba Formation, overlies Wiperaminga Subgroup, intruded by Lady Louise Suite|Fine-medium grained metasediments with variable calcareous compositions. Metasediments are pelitic and psammopelitic interspersed with psammitic, feldspathic and calcareous rocks. Intercalated felsic volcanics. Highly magnetic.|
35883|Ethiudna Subgroup|70657|4|Described|p10 Fig.4, p12, p13 Fig.6, p14-18,p20-32|Statherian|Statherian|See also p36-38, p41, p45-48, p51, p59-61, p63-66. Curnamona Province; Olary, Mulyungarie Domains. Relatively thin unit. Shows textural evidence of evaporite deposition. Shown as Ethiudna Subgroup + Redan Gneiss p10 Fig.4. Lack of outcrop has hindered geological understanding. Mis-spelt as Ethiudina Subgroup on p19. Contains Basso Suite extrusive units. Mn-rich units common (described); Cu-Au anomalous. Mineralisation described in some detail. Ca-Fe alteration mentioned. May be equivalent to Cues Formation.|~1715 Ma|Curnamona Group|Waukaloo, Whey Whey, Peryhumuck, Toraminga, Bewooloo, Cathedral Rock Formations.|Overlies Tommie Wattie and George Mine Formations. Is overlain by Bimba Formation in Olary Domain, and Thackaringa Group in Mulyungarie Domain. Intruded by Lady Louise Suite.|Lithologically diverse, but characterised by variable carbonate-calcsilicate, pyrite and fine-grained albitic psammite lithologies. Semi-stratabound calcsilicate-matrix breccia masses characteristic.|
35883|Ethiudna Subgroup|70658|5|Briefly described|p3, 5-6, 9, 15-16, 19, 23, 25, 29, 42|Paleoproterozoic|Paleoproterozoic|Olary Domain, Curnamona Province. Hosts Cu-Au mineralised thin layer-parallel magnetite+pyrite bodies.||Curnamona Group.|Tommie Wattie, Cathedral Rock, Toraminga, Whey Whey, Peryhumuck, Waukaloo Formations.|Overlies George Mine Formation (Wiperaminga Subgroup).|Includes thin clean detrital quartzites, feldspathic metasiltstone, thin calc-silicate units, and quartz-magnetite rock.|
35883|Ethiudna Subgroup|72461|6|Mentioned|p6||||c. 1710 Ma|||||
35883|Ethiudna Subgroup|73429|5|Briefly described|p106 Fig.2, p107-108|Statherian|Statherian|Curnamona Province, Olary Domain. Top of Ethiudna Subgroup approximates the regional redox boundary, interpreted as a regional unconformity. Deposited in chemically oxidised environment.||Curnamona Group||Overlies Wiperaminga Subgroup, unconformably underlies Bimba Formation, Larry Macs Subgroup|Dominated by fine-grained psammitic schists with variable carbonate, albite and calc-silicate.|
36782|Eucarro Rhyolite|24346|3|Fully described|p103|||Supersedes "Eucarro Dacite" and now includes the former "Nonning Rhyodacite", "Yannabie Rhyodacite" and "Paney Rhyodacite".  Defined as Eucarro Rhyolite Formation in Appendix 1.||||||
36782|Eucarro Rhyolite|24356|3|Fully described|p1592-1608|Mesoproterozoic|Mesoproterozoic|Of the upper part of Gawler Range Volcanics.  Compositionally zoned rhyolite lava with higher silica content at base; generally plagioclase rich and evenly porphyritic.  Conformably overlain by Yardea Dacite. Geological Province: Gawler Craton.||||||24-JAN-06
36782|Eucarro Rhyolite|65221|5|Briefly described|p28 Fig.3a |Mesoproterozoic|Mesoproterozoic|Of Gawler Range Volcanics||||||
36782|Eucarro Rhyolite|65922|5|Briefly described|p21|Calymmian|Calymmian|Supersedes Nonning Rhyodacite, Eucarro Dacite and Yannabie Rhyodacite. This article primarily uses the older names. Allen et al. (2003) suggest that this unit is wholly lava, not ignimbrite, in origin.||||||
36782|Eucarro Rhyolite|66302|6|Mentioned|p33|||||||||
36782|Eucarro Rhyolite|67028|5|Briefly described|p366|Calymmian|Calymmian|Of McPhie et al (2008)? Misnaming of Eucarro Dacite? Information on magnetic characteristics presented.||Gawler Range Volcanics||||24-APR-12
36782|Eucarro Rhyolite|67909|6|Mentioned|p137-138, 140-141|||Melt inclusion experiment results discussed.||Gawler Range Volcanics, upper.||||
36782|Eucarro Rhyolite|68158|5|Briefly described|p4|||||Gawler Range Volcanics.|||Massive, red to pink, columnar-jointed rhyolite; euhedral phenocrysts of plagioclase, olivine, pyroxene and hornblende; rare free quartz.|
36782|Eucarro Rhyolite|70659|5|Briefly described|p6 fig 2, p8-10|Mesoproterozoic|Mesoproterozoic|||Upper Gawler Range Volcanics.|Paney, Yannabie, Nonning, Rhyolite Members.|Overlies Roopena Basalt.||
36782|Eucarro Rhyolite|70816|4|Described|p1,3,5-7,17, 19|Mesoproterozoic|Mesoproterozoic|Geological province:  Spencer Domain, Gawler Craton. Gawler Ranges. Lithological description from RC 1 drill core. This unit outcrops extensively.||Lowermost flow of upper Gawler Range Volcanics.|Includes Paney, Yannabie and Nonning Rhyolite Members.|Overlies the Roopena Basalt.|Porphyritic rhyolite; plagioclase feldspar phenocrysts in a red-brown devitrified granophyric groundmass (K-feldspar intergrown with quartz, minor disseminated iron oxides). Plagioclase phenocrysts are altered to finely divided sericite and clay.|30-MAY-19
36782|Eucarro Rhyolite|70948|4|Described|p974-975, 977-981,984-985|Mesoproterozoic|Mesoproterozoic|Geological province: Gawler Craton. Porphyritic lava with a black glassy base, spherulitic to granophyric and columnar-jointed flow middle, and amygdaloidal flow top. Detailed mineralogical analysis described.||Unit of upper Gawler Range Volcanics.|||Porphyritic rhyolite composed of plagioclase phenocrysts in a red-brown devitrified granophyric groundmass of potassic feldspar intergrown with quartz and minor disseminated iron oxides.|
36782|Eucarro Rhyolite|71037|5|Briefly described|p22-23 Fig.2, p24, p27 Fig.6|Mesoproterozoic|Mesoproterozoic|Shown as the only constituent of the upper Gawler Range Volcanics in this area.||Gawler Range Volcanics (Upper)||Shown as younger than Spearfelt Rhyodacite and older than Gawler Range Volcanics.|Rhyolite, massive, red to pink, columnar-jointed, euhedral phenocrysts of plagioclase, pyroxene and hornblende, rare free quartz.|
36782|Eucarro Rhyolite|71129|4|Described|p47,85,88-91,184,190,207,225,227|Calymmian|Calymmian|Geological Province: Gawler Craton. Outcrops northwest of the Uno Fault on the hanging wall (and possibly correlative Nonning Rhyodacite outcrops on the foot wall of the Uno Fault), clustering around Four Mile Creek to the NW of Anzac Dam, and intersected in drillholes in the Burks Hutt area. Thickness: few meters in outcrop, up to 25.5m in drillhole, and estimated to be 200-300m elsewhere in Gawler Ranges. Probably deposited as a subaerial lava flow.||Gawler Range Volcanics||Overlain unconformably by Pandurra Formation. Correlable with Nonning Rhyolite. Faulted agains the Spearfelt Rhyodacite.|Reddish-brown, massive, feldspar-phyric rhyolite lava.|13-NOV-19
36782|Eucarro Rhyolite|71130|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|||Upper Gawler Range Volcanics.|||Red to pink, massive, columnar-jointed rhyolite with euhedral phenocrysts of plagioclase, pyroxene and hornblende, rare free quartz.|
36782|Eucarro Rhyolite|71131|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|||Upper Gawler Range Volcanics.|||Red to pink, massive, columnar-jointed rhyolite with euhedral phenocrysts of plagioclase, pyroxene and hornblende, rare free quartz.|
36782|Eucarro Rhyolite|71235|6|Mentioned|p7, p19|||||||||
36782|Eucarro Rhyolite|71317|4|Described|p1, p20, p23, p25-p35, p39|Mesoproterozoic|Mesoproterozoic|Age is a CA-TIMS age of magmatic crystallisation. Originally the Eucarro Dacite by Blissett (1986 and 1987) before being redefined as the Eucarro Rhyolite by Allen and McPhie, 2002; Allen et al., 2003). Distributed over a wide area in the western part of the Peltabinna Map Sheet area and forms prominent hills. Petrography discussed briefly. Estimated to be about 300-350m thick. Intruded by felsic dykes in the northwest of Peltabinna. See also p45-p46, p48-p58, p85, p96, p98, p104, p112-p114, p116-p117, p150, p153-p154, p156, p165-p166, p168-p169, p173, p176, p191-p192|1587.5 A+/- 0.6 Ma (Jagodzinski et al., 2016)|Gawler Range Volcanics|Includes the Yannabie Rhyolite Member, Paney Rhyolite Member.|Overlies the Bittali Rhyolite. Locally overlain by or intercalated with the Mount Friday Formation. Overlain by the Pondanna Dacite Member (Yardea Dacite). Intruded by the Hiltaba Granite.|Reddish-brown, columnar jointed, porphyritic rhyolite.|
36782|Eucarro Rhyolite|71414|6|Mentioned|p42 Fig 1|Mesoproterozoic|Mesoproterozoic|Geological province: Gawler Craton.||Unit of Gawler Range Volcanics.||||
36782|Eucarro Rhyolite|71559|4|Described|p16-p17, p19-20, p22-23|Mesoproterozoic|Mesoproterozoic|Geological province: Gawler Craton.||Unit of Upper Gawler Range Volcanics.||Intercalated with the Mount Friday Formation.|Rhyolite, massive, red, columnar-jointed; porphyritic with phenocrysts of feldspoar, pyroxene and hornblende, and rare free quartz in a spherulitic to granophyric groundmass.|19-JUN-19
36782|Eucarro Rhyolite|71560|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|||Upper Gawler Range Volcanics.|Yannabie, Paney Rhyolite Members.||Rhyolite, massive, red, columnar-jointed; porphyritic with phenocrysts of feldspar, pyroxene and hornblende, and rare free quartz in a spherulitic to granophyric groundmass.|16-APR-18
36782|Eucarro Rhyolite|72065|4|Described|p105-110,112-116,119|Calymmian|Calymmian|Geological province: Gawler Craton. Also shown as Eucarro Rhyolite Formation. Lava type: Strongly ferroan, alkali-calcic. Emplaced in >1My from around 1588 Ma (Jagodzinski et al., 2016). The first of at least three widespread felsic unit erupted in central and southern Gawler Ranges. Dimensions: >673km3, ~300m thick. Extensive rhyolite lava, presently exposed between the Bitalli Rhyolite and Pondanna Dacite to the S and N respectively. See major- and trace-element composition plots on p108 Fig 5. Contains 'GRV-type' crystal clusters: pyroxene and Fe-Ti oxides+\-apatite+\-zircon+\-plagioclase. Crystal formation likely formed from the most evolved of the Upper GRV parental melt (likely hot, dry, and relatively reduced, as pyroxenes predominate over biotite), after forming the Moonaree and Pondanna dacite crystals. Interpreted that crystals formed within the magmatic system, and required a subsequent event or rejuvenation (magma recharge: increased temperature or melt volatile content for example) to free the crystal clusters prior to, and during extrusive unit emplacement.||Unit of Gawler Range Volcanics.|Includes Paney and Yannabie rhyolite members.|Overlain by Pondanna Dacite Member. Intermingled with and overlain by the Paney Rhyolite Member.|Feldspar-phyric rhyolite; three main textural facies: dark-coloured base, central pink or red granophyre, and spherulitic and amygdular margins.|10-JAN-20
36782|Eucarro Rhyolite|72089|5|Briefly described|p2-p3|||Gawler Craton.  Rapidly erupted.||Gawler Range Volcanics, upper|||Rhyolitic lava.|
36782|Eucarro Rhyolite|72090|4|Described|p12, p50, p55, p57-p59|||Gawler Craton. Intersected in drillhole MSDP10. Calcite veins occur sporadically and are sometimes accompanied by quartz and chlorite. Fluorite veining has also been noted in places. Additional samples are described. Magnesium content increases towards the base. In contact with the Hiltaba Suite, although the nature of this contact is not made clear. See also p67-p68, p98, p100, p110.|1586.7 +/- 0.5 Ma|Gawler Range Volcanics, Upper|Includes the Paney Rhyolite Member, Yannabie Rhyolite Member and Nonning Rhyolite Member.|Overlain by the Pondanna Dacite Member and the Bittali Rhyolite.|Moderate reddish brown, porphyritic, fine- to medium-grained felsic lava.|
36782|Eucarro Rhyolite|72237|5|Briefly described|p29|Mesoproterozoic|Mesoproterozoic|Geological province: Gawler Craton.||Unit of Gawler Range Volcanics.||||
36782|Eucarro Rhyolite|72462|6|Mentioned|p8|||||||||
36782|Eucarro Rhyolite|73104|6|Mentioned|p3|Mesoproterozoic|Mesoproterozoic|||||||
36782|Eucarro Rhyolite|73110|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic||||Nonning, Paney, Yannabie, Rhyolite Members.||Rhyolite, massive, red to pink, columnar jointed, euhedral phenocrysts of plagioclase, olivine, pyroxene and hornblende, rare free quartz.|
36782|Eucarro Rhyolite|73162|6|Mentioned|p450 Fig.2|Mesoproterozoic|Mesoproterozoic|||||||
27401|Eudunda Arkose Member|22510|5|Briefly described|table1p37|Adelaidean|Adelaidean|Of the Tapley Hill Formation.  Age: Sturtian. Southwestern Flinders Ranges.||||||13-OCT-04
27401|Eudunda Arkose Member|29837|4|Described|p61|||||||||
27401|Eudunda Arkose Member|30801|6|Mentioned|p5|||Tapley Hill Formation. Table P5-6||||||
27401|Eudunda Arkose Member|30807|6|Mentioned|p103|||Suggested map symbol||||||
27401|Eudunda Arkose Member|34536|6|Mentioned|Map legend|Precambrian|Precambrian|Sturtian||||||
27401|Eudunda Arkose Member|34959|6|Mentioned|p285|||||||||
27401|Eudunda Arkose Member|40442|6|Mentioned|p10|||||||||
27401|Eudunda Arkose Member|41405|4|Described|p166|||||||||
27401|Eudunda Arkose Member|42243|6|Mentioned|p211|||||||||
27401|Eudunda Arkose Member|43052|5|Briefly described|p189|||of Tapley Hill Formation||||||
73285|Eumeralla Supersequence|63134|2|Defined|101|||||||||
73285|Eumeralla Supersequence|63269|5|Briefly described|p605-606, p609, p616, p618, p622-624|Early Cretaceous|Early Cretaceous|Otway Basin. Most oil-prone coals and shales are near the base. Oil-source correlation.|<115 Ma.|||Overlies Crayfish Supersequence. Is overlain by Shipwreck Supersequence.||
73285|Eumeralla Supersequence|69297|6|Mentioned|p77, p80, p81, p83, p96-p101|Lower Cretaceous|Lower Cretaceous|Nelson Sub-basin of the Otway Basin. Deposited in a fluvial or lacustrine environment. Interpreted from seismic data. See also p110, p114, p120, p370.||||||
73285|Eumeralla Supersequence|69651|5|Briefly described|p6, p10, p12-15, p17-19, p23, p25-26,p31|Albian|Early Cretaceous|See also p36-40, p42-44, p47, p49-50. Krassay et al. (2004). Otway Basin. Part of the Otway Supergroup. Potential source rocks. Fluvial to lacustrine deposits. Modelling diagrams.||||Overlies Crayfish Supersequence. Is overlain by Shipwreck Supersequence.|Argillaceous sandstone with interbedded claystone.|17-JUN-20
73285|Eumeralla Supersequence|70077|5|Briefly described|Nelson: p1. Regional: Fig.4; p3-4, p6-7|Early Cretaceous|Early Cretaceous|See also Regional: p9, p11 . Non-marine, fluvio-lacustrine deposits. A thick growth wedge in the ENE-trending Nerita Trough. Good potential source and reservoir rocks. Sealed by Eumeralla Formation shales both laterally and vertically.||||||
73285|Eumeralla Supersequence|70078|5|Briefly described|Regional: Fig.4; p3-4|Early Cretaceous|Early Cretaceous|Hosts part of Austral 2 petroleum system in Otway Basin. Seismic interpretation suggests it is present in the Sandy Cape Sub-basin.||||Is overlain by Shipwreck Supersequence.|Fluvial and lacustrine rocks, including coaly facies.|
73285|Eumeralla Supersequence|70880|5|Briefly described|p76-77, 81-83|Albian|Aptian|Otway Basin. Thins to the W and N. The likely source rock for gas accumulations in eastern Otway Basin. Is ~2.3 km thick in onshore Victoria; thickens slightly to the S until the shelf-edge break where it noticeably thins. Top surface is a major Basin-wide unconformity.||||Unconformably overlies Crayfish Supersequence. Is overlain unconformably by Shipwreck Supersequence.|Dominantly fluvio-lacustrine strata with a volcaniclastic sediment source.|
73285|Eumeralla Supersequence|71266|5|Briefly described|p614 Fig.3, p616-617, p620, p622 Fig.10|Early Cretaceous|Early Cretaceous|Otway Basin. Post-rift, thermal subsidence deposits. May be the source rock for gas accumulations in the eastern Otway Basin. Affected by faults; their growth is discussed in great detail.||||Overlies Crayfish Supersequence. Is overlain unconformably by Shipwreck Supersequence.|Fluvio-lacustrine deposits with evident volcaniclastic influence.|
36791|Euralia kimberlite|23772|5|Briefly described|p764||Jurassic|Gawler Craton. Age: 170 Ma.||||||
25901|Eurinilla Formation|23154|6|Mentioned|Map Legend|Holocene|Pleistocene|Geological Province - Lake Eyre Basin - Callabonna Basin.||||||
25901|Eurinilla Formation|23155|6|Mentioned|p36|||The unit is not recognised on STRZELECKI but can probably be equated with the Yandruwantha Sand.||||||
25901|Eurinilla Formation|30056|2|Defined|p145|Pleistocene|Pleistocene|||||||
25901|Eurinilla Formation|30920|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
25901|Eurinilla Formation|35619|6|Mentioned|p309|||||||||
25901|Eurinilla Formation|35691|6|Mentioned|p5|||||||||
25901|Eurinilla Formation|36620|5|Briefly described|Fig.1|||See also P24.||||||
25901|Eurinilla Formation|38605|6|Mentioned|p31|||||||||
25901|Eurinilla Formation|38682|5|Briefly described|p3|||||||||
25901|Eurinilla Formation|39085|6|Mentioned|p13|||||||||
25901|Eurinilla Formation|39804|6|Mentioned|Fig.2|||||||||
25901|Eurinilla Formation|40756|6|Mentioned|Fig.1.2|||||||||
25901|Eurinilla Formation|40914|6|Mentioned|Map legend|Cenozoic|Cenozoic|||||||19-NOV-08
25901|Eurinilla Formation|40926|6|Mentioned|Table 3|||||||||
25901|Eurinilla Formation|41125|6|Mentioned|Table 10|||||||||
25901|Eurinilla Formation|41537|6|Mentioned|Fig.2|||||||||
25901|Eurinilla Formation|42090|3|Fully described|p39|||||||||
25901|Eurinilla Formation|42205|6|Mentioned|Fig.1 P248|||||||||
25901|Eurinilla Formation|42720|6|Mentioned|map legend|Pleistocene||||||||
25901|Eurinilla Formation|42746|5|Briefly described|p23, Fig.9 p14|||of Lake Frome.||||||
25901|Eurinilla Formation|42784|6|Mentioned|p494|||||||||
25901|Eurinilla Formation|44133|5|Briefly described|p247, 244 Table 11.3, 242|Late Pleistocene|Late Pleistocene|Maximum Thickness: 10m. Equivalent to Pooraka Formation. ||||||
25901|Eurinilla Formation|46815|6|Mentioned|p250|||Refers to type sections.||||||
25901|Eurinilla Formation|46833|6|Mentioned|Fig.2|||||||||
25901|Eurinilla Formation|60953|5|Briefly described|Map Legend|Pleistocene|Pliocene|Fluvial and fluviolacustrine sediments.||||||28-APR-05
25901|Eurinilla Formation|61108|5|Briefly described|map legend|Pleistocene|Pliocene|Fluvial and fluviolacustrine sediments: channel sand, clay, some vertebrate fossils; often gypsified.||||||01-JUN-05
25901|Eurinilla Formation|61155|5|Briefly described|p17|Pleistocene|Pleistocene|Overlies Milyera Formation; overlain by Coonarbine Formation. Age: <1.5Ma. Geological Province: Tarkarooloo Basin.||||||
25901|Eurinilla Formation|65925|5|Briefly described|p18, Appendix 2.|||Northern Callabonna Sub-basin and near Lake Frome. Deposited partly in paleochannels formed within Willawortina Formation. Intermittent stream and overbank deposits. Up to 10m thick.||||Intertongues with Millyera Formation.|Bright red-brown to yellow-brown sand and gravel.|
25901|Eurinilla Formation|66131|6|Mentioned|p240, p244 Fig.4, p246-247|Pleistocene|Pleistocene|||||Correlative unit containing facies similar to the Katipiri Formation.||
25901|Eurinilla Formation|66518|6|Mentioned|p19 Fig.4.|Cenozoic|Cenozoic|Lake Eyre Basin.||||Overlies Willawortina Formation. Is overlain by Coonarbine Formation and equivalents. Is shown as age-equivalent to upper part of Millyera Formation.||
25901|Eurinilla Formation|68068|5|Briefly described|Map legend|Late Pleistocene|Early Pleistocene|Callabonna Sub-basin, Lake Eyre Basin. Bottom unit has vertebrate remains. Piedmont slope deposit, younger than Willawortina Formation. ||||Interdigitates with Millyera Formation.|Basal unit of conglomerate cemented by groundwater carbonate, gypseous mottled clays; middle unit of poorly-bedded pale orange sand and silt capped by calcareous palaeosol; top unit of widespread reddish to orange silty sand.|
25901|Eurinilla Formation|69023|5|Briefly described|p101, p109, p127-128|Pleistocene|Pleistocene|Defined by Callen and Tedford (1976). Represents a younger piedmont slope deposit. Late Pleistocene vertebrate fossils listed.||||Overlies Willawortina Formation.|Basal conglomerate cemented by carbonate, and poorly-sorted coarse-grained, yellowish-brown sand; overlain by reddish silty facies, a weak calcareous paleosol horizon, then reddish sand; a paleosol capping has carbonate nodules and some gypsum.|
25901|Eurinilla Formation|69654|6|Mentioned|p4|||Curnamona Province.||||||
25901|Eurinilla Formation|70339|5|Briefly described|map legend|Pleistocene|Pleistocene||||||Sand and gravel, alluvial, lacustrine, lacustrine shoreline, red-brown to yellow-brown.|
25901|Eurinilla Formation|70340|5|Briefly described|map legend|Pleistocene|Pleistocene||||||Sand and gravel, alluvial, lacustrine shoreline, red-brown to yellow-brown.|
25901|Eurinilla Formation|70384|5|Briefly described|Map legend.|Pleistocene|Pleistocene|Piedmont slope deposit; younger than Willawortina Formation. Early to late Pleistocene age range is inferred from fossil evidence.|||||Basal conglomerate cemented by groundwater carbonate, with mottled gypseous clays and vertebrate remains; poorly- to cross-bedded pale orange sand and silt capped by a calcareous paleosol; at the top a more widespread, reddish to orange silty sand.|
25901|Eurinilla Formation|73251|6|Mentioned|p36-37, p62|Holocene|Holocene|Lake Eyre Basin, Callabonna Sub-basin / Poontana Trough. Thermally sub-mature. Fluvial to fluviolacustrine depositional environments.||||Underlain by Willawortina Formation. Overlain by Coonarbine Formation. Equivalent to Millyera Formation.||
78810|Euro Limestone|64137|6|Mentioned|p1555 Tb.5|||Paxton Granite sampled near contact with Euro Limestone. Sampled in GP005D at 101.37 m. Overlying sample in same hole described as Tarcoola Formation limestone, and Fig.6 p1549 shows drill trace for GP005D going through Tarcoola Formation and into Paxton Granite.||||||21-JAN-22
69764|Ewarara Pyroxenite|61339|6|Mentioned|Map legend|||Mentioned in relation to ultramafic plugs and stocks in the Ewarara area.||||||
23585|Fabian Quartzite Member|22629|6|Mentioned|p158|||||||||
23585|Fabian Quartzite Member|23124|6|Mentioned|p397|||||||||
23585|Fabian Quartzite Member|39905|5|Briefly described|p4|||||||||
23585|Fabian Quartzite Member|41995|5|Briefly described|p12|||||||||
23585|Fabian Quartzite Member|42465|5|Briefly described|Map Legend|||||||||
23585|Fabian Quartzite Member|42469|3|Fully described|p13|||||||||
23585|Fabian Quartzite Member|43052|4|Described|p69|||of Tarcoola Formation||||||
23585|Fabian Quartzite Member|44935|5|Briefly described|Map Legend||Proterozoic|||||||
23585|Fabian Quartzite Member|50605|5|Briefly described|p8.6|||Of the Tarcoola Formation. Geological Province: Gawler Craton & Curnamona Province.||||||
23585|Fabian Quartzite Member|60704|5|Briefly described|p687, p688 Fig. 2|Paleoproterozoic|Paleoproterozoic|Of the Tarcoola Formation. Contains thin, laminated carbonates (stromatolites), overlain by thin- to thick-bedded, well-sorted quartzite and carbonaceous, pyritic, micaceous quartzite. Interbedded with "slates" of the Sullivan Shale Member.||||||07-NOV-08
23585|Fabian Quartzite Member|63276|5|Briefly described|p3 Fig. 2, p14 Fig. 3,|Proterozoic|Proterozoic|Of the Tarcoola Formation. Well-sorted quartzite with thin carbonate horizons. See also p5 Fig. 4.||||||
23585|Fabian Quartzite Member|64137|5|Briefly described|p1543 Fig.2, p1544, p1545 Fig.4 |Paleoproterozoic|Paleoproterozoic|Resistant; ridge-forming.||Of the Tarcoola Formation.||Is interbedded with Sullivan Shale Member.|Contains thin, laminated carbonates (stromatolites), overlain by thin to thick bedded (<2m), well-sorted quartzite and carbonaceous, pyritic, micaceous quartzite.|
23585|Fabian Quartzite Member|66302|5|Briefly described|p23|||Wilgena Domain, Gawler Craton. Deposited in a fluvial to marginal marine setting. ||Tarcoola Formation||Overlies the Peela Conglomerate. Overlain by the Sullivan Shale Member.|Quartzites and sandstones.|
23588|False Bay Formation|40976|6|Mentioned|Table 1|||||||||
23588|False Bay Formation|44133|6|Mentioned|p228, 228 Fig. 11.7|||||||||
23588|False Bay Formation|62577|6|Mentioned|p566, p571|Late Pleistocene|Late Pleistocene|||||||
23588|False Bay Formation|70334|4|Described|p3,61-64,66,83|||Of Spencer Gulf area. Thickness: 50cm to 3.5m thick on CULTANA. Not exposed on CULTANA, but intersected in vibrocores in Spencer Gulf where water depths exceed 8m. Underwent local erosion or non-deposition in the gulf prior to Lowly Point Formation deposition. Transgressive marine unit, terminated by marine regression, sub-aerial exposire and pedogenesis. Contains a palaeosol defined by a calcareous horizon and evidence of aeolian reworking. Deposited in estuarine to lagoonal environments at around 105ky after the last interglacial maximum (OIS 5c; Hails et al., 1984b).||||Overlain by Lowly Point Formation. Underlain by Mambray Formation.|Poorly consolidated beach sands, yellowish-green to reddish brown oxidised fine-grained sandy and silty clays and white grey to buff wackestone and bryozoan limestone; fossils of foraminifera, juvenile bivalves, bryozoa and sponge spicules.|14-OCT-19
29839|Faugh-a-Ballagh Member|22884|2|Defined|p40 Fig. 1, p42-3||Paleoproterozoic|Of Tommie Wattie Formation (Thackaringa Group). Underlain by Morialpa Migmatite. Max. thickness is 1000m. Calc-albitite and plagioclase-rich metasediment in quartzofeldpsthic metasediment; minor amphibolite and ironstone.||||||26-MAR-09
29839|Faugh-a-Ballagh Member|70339|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|||probably of Peryhumuck Formation.|||Calc-albitite and plagioclase-rich metasediment in quartzofeldspathic metasediment; minor amphibolite and ironstone.|
29839|Faugh-a-Ballagh Member|70405|4|Described|p23|Paleoproterozoic|Paleoproterozoic|Originally defined as a member of the Tommie Wattie Formation.||Peryhumuck Formation|||Fine grained psammite of calc-albitic composition commonly containing epidote. Also present is rippled, flaser bedded alkalifedsparite, K-feldsparite with biotite, laminated epidote rich metasiltstone.|
75865|Finlay Dam Rhyolite|67540|3|Fully described|p25, pp27-28, p36 Tb.3, p38 Fig.2|Calymmian|Calymmian|Type locality: Drillhole Mudguard 1, between 192-204m. Definition reference: this article and Fricke and Hore (2011). Curnamona Province: Mudguard Domain and Moorowie Sub-basin - Erudina Domain. Another age is 1581 +/- 4 Ma (SHRIMP: Fanning et al., 1998).|1587+/-6 Ma (SHRIMP II: Jagodzinsk & Fricke,2010)|Of the Benagerie Volcanic Suite.|||Porphyritic, K-feldspar (orthoclase)-plagioclase-quartz rhyolite with apatite, zircon and minor fluorite and hematite-sericite-carbonate alteration. A-type.|08-SEP-14
75865|Finlay Dam Rhyolite|67900|6|Mentioned|p20|||||Benagerie Volcanic Suite.||Unconformably overlies Willyama Supergroup.||
75865|Finlay Dam Rhyolite|69562|5|Briefly described|p672 Tb.5||||1587 +/- 6 Ma (Jagodzinski and Fricke, 2010).|Unit in Benagerie Volcanic Suite.|||Porphyritic rhyolitic volcanic rocks.|
75865|Finlay Dam Rhyolite|69650|2|Defined|p4 Tb.1, p7, p11, p13, p44, p46 Fig.2|Calymmian|Calymmian|See also p47-50. New name, after Finlay Dam. Type section: Drillhole Mudguard 1, GDA 94, 449389 mE, 6596300 mN (Fig. 20), within the interval 192?204 m. Geophysical imagery suggests a thick, flat-lying sheet. SHRIMP II age; also 1581 +/- 4 Ma (SHRIMP U-Pb zircon, Fanning et al. 1998). Geochemistry detailed.|1587 +/- 6 Ma; Jagodzinski and Fricke, 2010.|Unit in Benagerie Volcanic Suite.||Unconformably overlies folded Willyama Supergroup. Gradationally interlayered with Lake Elder Rhyodacite.|Red, porphyritic, orthoclase-plagioclase-quartz rhyolites with apatite, zircon and minor fluorite and hematite-sericite-carbonate alteration. A-type.|25-NOV-22
75865|Finlay Dam Rhyolite|70658|5|Briefly described|p33-35, 37|Mesoproterozoic|Mesoproterozoic|Curnamona Province. Geochemistry briefly described. Distribution sites listed.|1587-1581 Ma.|Benagerie Volcanic Suite.|||Porphyritic, orthoclase-plagioclase-quartz rhyolite with apatite, zircon and minor fluorite and hematite-sericite-carbonate alteration. A-type.|
31518|Finniss Formation|23179|6|Mentioned|Fig.2|Middle Miocene|Early Miocene|Of the Murray Supergroup.  Geological province: Murray Basin.||||||05-FEB-08
31518|Finniss Formation|23226|4|Described|p896|Batesfordian|Longfordian|Was the Finniss Clay.  Of Murray Supergroup.||||||
31518|Finniss Formation|24558|4|Described|p655 Fig. 3|Early Miocene|Early Miocene|Low energy carbonate ramp sediments with with abundant molluscs. Conformably overlies Mannum Formation; conformably overlain by Glenforslan Formation.||||||12-APR-05
31518|Finniss Formation|63460|4|Described|p839 Fig. 2b|Early Miocene|Early Miocene|Basal unit of Morgan Subgroup. Includes Cowirra Clay and Portee Carbonate Members, Woolunda Marl Member. Overlies Mannum Fm; underlies Glensforlan Fm. Merges laterally with Ettrick Fm. Thick: 50m. Geol.prov: Murray Basin. Clay, marl + calcarenite lithology, with marl dominating.||||||08-SEP-20
31518|Finniss Formation|64237|5|Briefly described|p18, p19|Early Miocene|Early Miocene|Replaced Finniss Clay in the Lukasik and James (1998) revision of the Murray Group up to Murray Supergroup.............modified name retained within Morgan Subgroup in reistated Murray Group. 3 new members also retained.||||||15-JUL-08
31518|Finniss Formation|68715|5|Briefly described|p31 Fig.5|Miocene|Miocene|Murray Basin. Middle Miocene age.||Of the Murray Group.||||
31518|Finniss Formation|72445|5|Briefly described|App.6 p2 Fig.1.|Early Miocene|Early Miocene|Of Gallagher and Gourlay (2007), Lukasik and James (1998). See also Finnis Clay, App.7.||Murray Supergroup||Overlies Mannum Formation and underlies Glensforian Formation.|Includes marl and marly limestone.|
31518|Finniss Formation|73228|6|Mentioned|p50, p55-57|Middle Miocene|Late Early Oligocene|Murray Basin, patchily distributed along the southwestern margin.||Murray Group||||
31518|Finniss Formation|73229|6|Mentioned|p67|Middle Miocene|Late Early Oligocene|Murray Basin.||Murray Group||||
29470|Fishing Bay Formation|42966|6|Mentioned|p179|||||||||
29852|Flinders Chase Granite|64282|5|Briefly described|Map legend|Middle Cambrian|Middle Cambrian|Part of Delamerian Orogeny.  Fine- to coarse-grained, grey quartz-feldspar-biotite granite; foliated around the margins.||||||02-JUL-08
29852|Flinders Chase Granite|73107|5|Briefly described|Map legend.|Middle Cambrian|Middle Cambrian|Delamerian Orogeny.|||||Fine to coarse-grained, grey, quartz-feldspar-biotite granite, foliated around the margins.|
25915|Freeling Heights Quartzite|22631|6|Mentioned|table1, p176|Calymmian|Calymmian|||||||
25915|Freeling Heights Quartzite|23394|5|Briefly described|Map legend|Proterozoic|Proterozoic|||||||
25915|Freeling Heights Quartzite|23411|6|Mentioned|Map Legend|||||||||
25915|Freeling Heights Quartzite|23775|5|Briefly described|p721|||Of Radium Creek Metamorphics.||||||22-SEP-09
25915|Freeling Heights Quartzite|23818|5|Briefly described|p35|||Underlying unit: Brindana Schist. Max. thickness: 13 000 ft. Intertongues with the Brindana Schist.||||||
25915|Freeling Heights Quartzite|24176|4|Described|p7, p26 Tb. 1|Proterozoic|Proterozoic|Of Radium Creek Metamorphics.  Feldspathic quartzites, arenaceous schists, mica schists, minor corundum schists, quartz pebbles, conglomerates; cross-bedding common.  Max. thickness: >4100m.  Geological Province: Mount Painter Province.||||||
25915|Freeling Heights Quartzite|24546|5|Briefly described|p2 - 3 Fig.2|Mesoproterozoic|Paleoproterozoic|Strongly foliated and recrystallized quartzite. Forms part of Mount Painter Basement of the Adelaide Fold Belt.||||||07-NOV-08
25915|Freeling Heights Quartzite|24593|6|Mentioned|p625 Fig. 8|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
25915|Freeling Heights Quartzite|30176|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
25915|Freeling Heights Quartzite|30177|2|Defined|p124|Paleoproterozoic|Paleoproterozoic|Type section: Three miles north-northwest of Freeling Heights, lat. 30degrees05'58"S long. 139degrees21'57"E to lat. 30degrees06'04"S long. 139degrees23'07"E Yudnamutana Creek, 2.8 miles south-southwest of Freeling Heights, lat. 30degrees 11'01"S long. 139degrees22'08"E to lat. 30degrees11'01"S long. 139degrees23'13"E. Two and a half miles north-northwest of Mount Adams, lat. 30degrees02'58"S long. 139degrees30'03"E to lat. 30degrees03'53"S long. 139degrees30'02"E.||||||24-NOV-22
25915|Freeling Heights Quartzite|30807|6|Mentioned|p103|||Suggested map symbol||||||
25915|Freeling Heights Quartzite|30920|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Prob.Lower Proterozoic||||||07-NOV-08
25915|Freeling Heights Quartzite|34537|6|Mentioned|p35|||||||||
25915|Freeling Heights Quartzite|35255|6|Mentioned|Fig.24|||||||||
25915|Freeling Heights Quartzite|41402|6|Mentioned|p38|||||||||
25915|Freeling Heights Quartzite|41403|6|Mentioned|p46|||||||||
25915|Freeling Heights Quartzite|42624|5|Briefly described|p30|||||||||
25915|Freeling Heights Quartzite|60953|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Sericitic feldspathic quartzite and schist, minor pelitic schist.||||||
25915|Freeling Heights Quartzite|61108|5|Briefly described|map legend|Mesoproterozoic|Mesoproterozoic|Sericitic feldspathic quartzite and schist, minor pelitic schist.||||||
25915|Freeling Heights Quartzite|62962|6|Mentioned|p2283 Fig. 1(c), p2284 Fig. 2, p2291|Paleozoic|Paleozoic|Geological Province: Mount Painter Province.||||||07-FEB-11
25915|Freeling Heights Quartzite|63489|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Included with undifferentiated quartzitic metasediments. Geological Province: Mount Painter Inlier.||||||10-SEP-07
25915|Freeling Heights Quartzite|66302|6|Mentioned|p39, p49, p77|Mesoproterozoic|Mesoproterozoic|Moolawatana Domain, Curnamona Province.|1595 to 1591 Ma|||||
25915|Freeling Heights Quartzite|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Mount Painter area.|1591 +/- 6 Ma (maximum depositional age).|||||
25915|Freeling Heights Quartzite|67430|6|Mentioned|p38|||Mount Gee - Mount Painter area, Mount Painter Inlier.|1600-1590 Ma (MDA; Fanning and Teale, 2003).|||||
25915|Freeling Heights Quartzite|67536|5|Briefly described|Map Legend|Calymmian|Calymmian|Curnamona Province.|ca. 1576 +/- 2 Ma - 1575 +/- 14 Ma||||Quartzitic, pelitic and calcsilicate metasediments; volcanic rocks at Gunsight and Harts Creek.|
25915|Freeling Heights Quartzite|67653|6|Mentioned|p4|||Geological province: Curnamona Province. |||||Strongly peraluminous two-mica granites with S-type affinities, although some components show weakly metaluminous compositions.|
25915|Freeling Heights Quartzite|69019|5|Briefly described|p14, p18|Calymmian|Calymmian|Mapping by Teale (1993) suggests that Pepegoona Porphyry and Freeling Heights Quartzite are not part of Radium Creek Metamorphics. Age from detrital zircons.|c.1590-1580 Ma max. (Fanning et al 2003).|||||
25915|Freeling Heights Quartzite|69023|5|Briefly described|p14, p16, p18, p27 Fig.8, p52|||Mount Painter Inlier. Parts of this unit have been removed from Radium Creek Metamorphics. Detrital zircon maximum deposition age.|~1590-1580 Ma (Fanning et al., 2003).|||||
25915|Freeling Heights Quartzite|69654|6|Mentioned|p3|||Curnamona Province.||||||
25915|Freeling Heights Quartzite|70383|5|Briefly described|p44|Mesoproterozoic|Mesoproterozoic|Maximum depositional age.|< c. 1600-1590 Ma.|Uppermost Radium Creek Group.||||
25915|Freeling Heights Quartzite|70384|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|West of Paralana Fault Zone. Maximum age from detrital zircons. Metamorphic rims dated at 1556 +/- 10 Ma (ICPMS).|<1590-1580 Ma (SHRIMP and ICPMS U-Pb).|Radium Creek Group.|||Meta-sandstone, medium- to coarse-grained, sericitic, feldspathic; grits; quartzite pebble beds; schist. Separately mapped: quartzite-pebble conglomerate interbeds; quartzite, highly radioactive as determined from aerial radiometric surveys.|
25915|Freeling Heights Quartzite|71531|14|Not recorded|p9|||No age.||||||
78746|Fresh Well Formation|70659|2|Defined|Throughout.|Mesoproterozoic|Mesoproterozoic|See also p28, p36, p40, p42, p57, p59, p60. Gawler Craton. Named after Fresh Well on Roopena Station. Originally equated with Corunna Conglomerate (Daly, 1993; Thomson, 1980). Type locality (722300 mE, 6374950 mN, GDA 94, zone 53) and reference drillhole details given. Up to 225m thick. Extensional crustal setting. Previously referred to informally as Roopena sequence and Fresh Well formation (SAMEDAN Oil Corporation of Australia, 1985). Lithological facies described and illustrated in great detail. Graphic core logs. Often abbreviated in the text to FWF.|1587 +/- 15 Ma (SHRIMP U-Pb zircon).|Lower Gawler Range Volcanics.||Conformably interlayered with Roopena Basalt. Overlain by Pandurra Formation. Overlies Wandearah and Moonabie Formations unconformably, and Angle Dam Volcanics (which also intrudes).|Fluvio-lacustrine volcaniclastic sequence of mudstone, siltstone, fine-coarse grained lithic sandstone, pebble conglomerate, three major ash fall tuff intervals and peperitic breccia.|
78746|Fresh Well Formation|70816|4|Described|p3-4,17-18, 19|Mesoproterozoic |Mesoproterozoic |Roopena-Myall Creek area, Gawler Ranges.  Up to 225 m thick over area 4x3 km.||Unit of lower Gawler Range Volcanics.||Conformably interlayered with Roopena Basalt. Intruded by Angle Dam Volcanics.|Volcaniclastic lacustrine sediments.|
78746|Fresh Well Formation|70948|5|Briefly described|p974, 975|Mesoproterozoic|Mesoproterozoic|Geological province: Gawler Craton.||Unit of lower Gawler Range Volcanics.|||Volcaniclastic lacustrine sediments.|
78746|Fresh Well Formation|71037|5|Briefly described|p22-23 Fig.2, p27 Fig.6, p27|Mesoproterozoic|Mesoproterozoic|U-Pb SHRIMP maximum depositional age 1587+/-15 Ma (Johnson, 1993). Lacustrine sediments.|1587 +/- 15 Ma.|Gawler Range Volcanics (Lower)||Peperitic contact with Angle Dam Volcanics. Overlain by Roopena Basalt.|Fine to medium-grained arkosic and lithic sandstone, massive to laminated siltstone, laminated dolomitic mudstone, pebble conglomerate and felsic tuff.|
78746|Fresh Well Formation|71129|3|Fully described|p35,47,69,71,73-75,82,84|Calymmian|Calymmian|Geological Province: Gawler Craton. Type locality: area extending 150m N and S, and 450m to the E and W around point 722300mE, 6374950mN (McAvaney and Wade, 2015b). Reference drillhole: Drillhole ROOPENA DDH 6 (19915), 724922 m E, 6376828 m N, between 20-105.58 m and 116.7256.76 m (McAvaney and Wade, 2015b). Also intersected in drillholes SAMEDAN SOC 1, SAMEDAN SOC 3, SAMEDAN SOC8, ROOPENA DDH 1,  ROOPENA DDH 3 and ROOPENA DDH 4.  Deposited in a tectonically active NS-trending graben-like basin. Bounded to the W and E by Roopena and Wizzo Well faults respectively, and to the S by Wandearah Formation outcrop and to the N by Roopena Basalt subcrop. Interlayered with Roopena Basalt, and divisible into upper and lower sections. Contains tuff dated at 1587+\-15 Ma (SHRIMP U-Pb; Johnson 1993), within error of other published dates from the GRV (Fanning et al., 1988, Creaser and Cooper, 1993, Fanning et al., 2007, Jagodzinski et al., 2016); and contains c. 1740 Ma zircons possibly derived from Worthan Granite or Gluepot Granite. See also p114,144,184, p188 ,201-202,206,225,227,230.||Unit of Gawler Range Volcanics.||Interlayered with Roopena Basalt. Underlain unconformably by Moonabie Formation or Wandearah Formation.|Cyclic, coarsening-upwards volcaniclastic sequences of mudstone, siltstone, fine- to coarse-grained lithic sandstone and pebble conglomerate, ash fall tuff and peperite.|13-NOV-19
78746|Fresh Well Formation|71130|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|SHRIMP U-Pb maximum depositional age.|< 1587 +/- 15 Ma (Johnson, 1993).|Lower Gawler Range Volcanics.||Peperitic contact with Angle Dam Volcanics.|Fine- to medium-grained arkosic and lithic sandstone, massive to laminated siltstone, laminated dolomitic mudstone, pebble conglomerate and felsic tuff.|
78746|Fresh Well Formation|71131|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|SHRIMP U-Pb maximum depositional age.|< 1587 +/- 15 Ma (Johnson, 1993).|Lower Gawler Range Volcanics.||Peperitic contact with Angle Dam Volcanics.|Fine- to medium-grained arkosic and lithic sandstone, massive to laminated siltstone, laminated dolomitic mudstone, pebble conglomerate and felsic tuff.|
78746|Fresh Well Formation|71414|6|Mentioned|p42 Fig 1, p43|Mesoproterozoic|Mesoproterozoic|Geological province: Gawler Craton. Up to 255m thick.||Unit of Gawler Range Volcanics.||Interlayered with Roopena Basalt.|Volcaniclastic fluviolacustrine sediments.|
78746|Fresh Well Formation|72089|4|Described|p2-p3, p21-p25, p27|||Gawler Craton. The lower part of this unit has a maximum known thickness >140m. The upper part of this unit is 85.6m thick. Deposited in fluvial and lacustrine environments.||Gawler Range Volcanics, lower||Intercalated with the Roopena Basalt. Intruded by the Angle Dam Volcanics.|Coarsening upwards sequence of mudstone, siltstone, lithic sandstone and volcaniclastic conglomerate.|
78746|Fresh Well Formation|72090|6|Mentioned|p12, p14, p34|||Gawler Craton.||Gawler Range Volcanics, Lower||||
78746|Fresh Well Formation|72237|5|Briefly described|p29,32|Mesoproterozoic|Mesoproterozoic|Geological province: Gawler Craton. Of Roopena Basin. Presence of localised hematite-chlorite-sericite (white mica) alteration is characteristic of hematite-style IOCG deposits and prospects within Gawler Craton.||Unit of Gawler Range Volcanics.||||
78746|Fresh Well Formation|73162|4|Described|p447-448, p450-455, p457-461|Mesoproterozoic|Mesoproterozoic|Roopena Basin. Upward-coarsening sequences and sharp basal contacts provide evidence of rapid flooding events. U-Pb SHRIMP maximum depositional age of 1587 +/- 15 Ma from tuff beds within Fresh Well Formation. Detrital zircon signature shows sedimentary input from the ca. 1635-1605 Ma St Peter Suite, and a minor component of Gawler Range Volcanic-aged zircon. Originally correlated with Corunna Conglomerate but this now considered distinctly older (< 1660 Ma) and they are defined as distinct stratigraphic units.|ca. 1580 Ma.|lower Gawler Range Volcanics|lower Fresh Well Formation, upper Fresh Well Formation including Whaler Hut Member, Stud Dam Member, Comet Bore Member.|Overlies the Angle Dam Dacite. Intercalated with units of the Roopena Basalt.|Volcaniclastic alluvial-fluvio-lacustrine packages of claystone, siltstone, lithic sandstone, conglomerate, tuff and breccia. Localised hematite-chlorite-sericite (white mica) alteration.|
78746|Fresh Well Formation|73234|6|Mentioned|p19|||Six Mile Hill area. Contemporaneous with Gawler Range Volcanics and Hiltaba Suite.|||||Volcano-sedimentary rocks.|
24637|Fulham Sand|22888|6|Mentioned|P36|||||||||
24637|Fulham Sand|23489|5|Briefly described|p47|||||||||
24637|Fulham Sand|23818|5|Briefly described|p212 Fig.108|Recent|Recent|Geological Province: Great Artesian Basin.||||||
24637|Fulham Sand|30176|6|Mentioned|Map legend|Recent|Recent|||||||
24637|Fulham Sand|30752|6|Mentioned|p2|||||||||
24637|Fulham Sand|30807|6|Mentioned|p101|||Suggested map symbol||||||
24637|Fulham Sand|31315|4|Described|p187|||Overlies calcrete horizons. Recent.||||||
24637|Fulham Sand|33422|6|Mentioned|Map legend|Cenozoic|Cenozoic|||||||19-NOV-08
24637|Fulham Sand|33423|6|Mentioned|p15|||Stratigraphy.||||||
24637|Fulham Sand|34180|6|Mentioned|p212|||Recent||||||
24637|Fulham Sand|34181|5|Briefly described|p46|||||||||
24637|Fulham Sand|34536|6|Mentioned|Map legend|Recent|Recent|||||||
24637|Fulham Sand|35097|6|Mentioned|Fig.4|||||||||
24637|Fulham Sand|35159|5|Briefly described|p12|||See also Fig.2.||||||
24637|Fulham Sand|35772|6|Mentioned|p14|||||||||
24637|Fulham Sand|36621|6|Mentioned|Fig.1|||||||||
24637|Fulham Sand|36623|6|Mentioned|Fig.1|||||||||
24637|Fulham Sand|38068|5|Briefly described|p79|||See also Fig.8.||||||
24637|Fulham Sand|40003|5|Briefly described|Table 11|||||||||
24637|Fulham Sand|40442|6|Mentioned|p38|||See also Fig.23.||||||
24637|Fulham Sand|41362|1|Redefined|p8|||||||||
24637|Fulham Sand|41506|6|Mentioned|p9|||||||||
24637|Fulham Sand|41943|6|Mentioned|Fig.3 P73|||||||||
24637|Fulham Sand|42733|5|Briefly described|map legend|Quaternary||||||||
24637|Fulham Sand|43053|5|Briefly described|Map Legend|Pleistocene|Pleistocene|Orange siliceous aeolian sand.||||||25-MAY-05
24637|Fulham Sand|43258|5|Briefly described|Map Legend|Holocene|Pleistocene|||||||
24637|Fulham Sand|43298|5|Briefly described|Map Legend|Holocene|Pleistocene|||||||
24637|Fulham Sand|44133|6|Mentioned|p230|||||||||
24637|Fulham Sand|44660|14|Not recorded|map legend|||Recent.||||||
24637|Fulham Sand|60953|5|Briefly described|Map Legend|Pleistocene|Pleistocene|Orange siliceous aeolian sand.||||||
24637|Fulham Sand|61108|5|Briefly described|map legend|Pleistocene|Pleistocene|Orange, siliceous aeolian sand.||||||
72709|Gairdner Dolerite|63224|5|Briefly described|p11||Neoproterozoic III|Formerly the Gairdner Dyke Swarm.  Geological Province: Gawler Craton.||||||07-FEB-08
72709|Gairdner Dolerite|64647|6|Mentioned|p46|||||||||
72709|Gairdner Dolerite|65221|5|Briefly described|p28 Fig.3a |Neoproterozoic|Neoproterozoic|||||||
72709|Gairdner Dolerite|65483|5|Briefly described|p19|Neoproterozoic|Neoproterozoic|Believed to be intrusive equivalent to Beda Volcanics. Age c. 825 Ma (Wingate et al 1998). Dykes of this unit intrude the northern part of the Cultana Subsuite.||||||28-JAN-11
72709|Gairdner Dolerite|65693|5|Briefly described|p4. |||Occurs in a series of dykes.|825 Ma.|||||
72709|Gairdner Dolerite|67375|4|Described|p54, p55, p262, p348.|Neoproterozoic|Neoproterozoic|Mostly NW- to N-trending; extend from the Gawler and Stuart Shelf to the Musgrave Province. Linked to Amata Dolerite (east Musgrave Province) on basis of similar chemistry and age. Metamorphosed during the Petermann Orogeny (c.570 to 550 Ma).|827 +/- 6 - 824 +/- 4 Ma (Glikson et al. 1996).|||Crosscuts the Warakurna Supersuite, Bentley Supergroup, Kullal Dyke Suite and norite of the Giles Suite.|Medium-grained, intergranular to subophitic dolerite; shows polygonal granoblastic texture where recrystallized.|
72709|Gairdner Dolerite|67553|5|Briefly described|p56,78-79|Tonian|Tonian|Geological province: Musgrave Province, North Australian Craton. Thickness: up to 150m at (BELL ROCK, MGA 481850E 7117850N). Crosscuts the c. 1000 Ma Kullal Dyke Suite and Giles layered intrusions.|c. 825 Ma||||Medium-grained, intergranular to subophitic dolerite.|
72709|Gairdner Dolerite|68067|6|Mentioned|Map legend.|||||||||27-AUG-13
72709|Gairdner Dolerite|68126|6|Mentioned|p29|Neoproterozoic|Neoproterozoic|||||||
72709|Gairdner Dolerite|68208|6|Mentioned|p32 Fig.3, p37|Neoproterozoic|Neoproterozoic|NW-trending anomalies in aeromagnetic data attributed to dykes of this unit.||||||
72709|Gairdner Dolerite|69003|5|Briefly described|p4, p59-60|Neoproterozoic|Neoproterozoic|West Musgrave Province, Paterson Orogen. Mantle plume activity associated with the break-up of Rodinia.|c.825 Ma.|||||
72709|Gairdner Dolerite|69019|5|Briefly described|p32-33, p78, p80-81 Figs.17,19, p142.|Neoproterozoic|Neoproterozoic|Forms a dyke swarm intruding the Gawler Craton. Described in comparison with Ooloo Hill Formation basalt.|827 +/- 6 Ma (baddeleyite: Wingate et al. 1998).|||||
72709|Gairdner Dolerite|69023|6|Mentioned|p55, p58|Neoproterozoic|Neoproterozoic|Forms a dyke swarm.||||||
72709|Gairdner Dolerite|69091|5|Briefly described|p77-78|||Extend from Gawler Craton and Stuart Shelf to Musgrave Province. c. 800 Ma event produced Gairdner Dolerite and Amata Dolerite.|c. 825 Ma|||Crosscuts Kullal Dyke Suite.||
72709|Gairdner Dolerite|69153|5|Briefly described|GEOCHRON/194759.1.pdf|Neoproterozoic|Neoproterozoic|Age mentioned in GEOCHRON/194759.1.csv file.|825 Ma, Glikson et al. 1996; Wingate et al. 1998|||cross-cuts Kullal Dyke Suite||24-MAR-16
72709|Gairdner Dolerite|69436|5|Briefly described|p21:15|||Howard et al. (2011). A dyke swarm which extends from the Gawler Range and Stuart Shelf in SA. Has similar age, geochemistry and eNd values to the Amata Dolerite.|||||Subophitic dykes with slightly enriched, primitive mantle-normalised, incompatible trace element geochemistry and eNd values of +2.39 and +3.81.|12-JUL-16
72709|Gairdner Dolerite|69648|5|Briefly described|p16|||Formerly Gairdner Dyke Swarm. Major swarm of dykes of variable magnetic character (dominated by positively magnetic dykes); generally trends NW-SE. Not recorded in any drilling on OOLDEA. Eastern Officer Basin.||||||17-FEB-15
72709|Gairdner Dolerite|69666|5|Briefly described|p24, p26-27, p33, p35-37|Neoproterozoic|Neoproterozoic|Part of the Willouran Basic Province. Intrudes central Gawler Craton. Inferred to be feeder dykes to the Beda Basalt and other volcanics of the Willouran Basic Province. Geochemistry described in some detail. Similar major and trace element abundances to Beda Basalt. Pb-Pb baddeleyite age.|827 +/- 7 Ma (Wingate et al., 1998).|||||
72709|Gairdner Dolerite|69729|5|Briefly described|p74 Fig.8, p84-86|Neoproterozoic|Neoproterozoic|Mostly NW-trending dykes extending from SE Gawler Craton to the west Musgrave Province. Trace element plot.|c.827-824 Ma.|||||
72709|Gairdner Dolerite|70333|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Other age determinations are Sm-Nd ages of 867 +/- 47 Ma and 802 +/- 35 Ma.|827 +/- 6 Ma (U-Pb).||||Dolerite dykes locally intruded by black basalt.|
72709|Gairdner Dolerite|70334|5|Briefly described|p2,10,14,42,44-47,76,83|Tonian|Tonian|Geological province: Gawler Craton. Dimensions: average 30km long, >50m wide (Flint et al., 1993). Consists of a swarm of NE-SW trending linear dolerite dykes, extends >1000 km in the Gawler Craton and Stuart Shelf (Parker et al., 1987, Preiss, 1987, Cowley and Flint, 1995), NW Musgrave Province (Zhao et al., 1994) and Broken Hill Domain (Hilyard, 1989, Crawford and Hilyard, 1990, Ernst et al., 2008). Age of intrusion constrained by SHRIMP U-Pb baddeleyite and zircon ages (827+\-6 Ma; Wingate et al., 1998), and Sn-Nd mineral isochrons (802+\-35 Ma and 867+\-47 Ma; Zhao et al., 1994).|827+\-6 Ma (U-Pb)|||Intrudes Moonabie and Pandurra formations, and Cultana Subsuite. Contemporaneous with Beda Basalt and Backy Point Formation; Littlle Broken Hill Gabbro.||14-OCT-19
72709|Gairdner Dolerite|70336|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|||||||
72709|Gairdner Dolerite|70339|5|Briefly described|map legend|Neoproterozoic|Neoproterozoic||Sm-Nd 867+/-47 and 802+/-35 Ma; U-Pb 827+/-6 Ma.||||Dolerite dykes locally intruded by black porphyritic basalt.|
72709|Gairdner Dolerite|70405|5|Briefly described|p79, p49|Neoproterozoic|Neoproterozoic||827 Ma ||||Mafic (metadolerite) dykes.|
72709|Gairdner Dolerite|70634|4|Described|100k_geologyp_lut,csv|Cryogenian|Cryogenian||824 Ma - 827 Ma||||Medium-grained dolerite and metadolerite; typically intergranular to subophitic; polygonal granoblastic where metamorphosed|
72709|Gairdner Dolerite|70658|6|Mentioned|p29|||||||||
72709|Gairdner Dolerite|70659|6|Mentioned|p10, p14, p375|Neoproterozoic|Neoproterozoic|Thin section description.||||||
72709|Gairdner Dolerite|70793|4|Described|GEOL_LUT_CSV files|Cryogenian|Cryogenian|Geological province: Paterson Orogen, Musgrave Province. Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma). See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 100k_interpgeol_lut.csv, 100k_geologyl_lut.csv, 250k_interpgeol_lut.csv, 500k_interpgeol_lut.csv, 2_5m_interpdykel15_lut.csv.|827+\-6 Ma; 824+\-4 Ma|||Intrudes into Kullal Dyke Suite.|Medium-grained dolerite and metadolerite; typically intergranular to subophitic; polygonal granoblastic where metamorphosed|
72709|Gairdner Dolerite|70819|6|Mentioned|p13|Neoproterozoic|Neoproterozoic|Clare Valley.|827 +/- 6 Ma (U-Pb).|||||
72709|Gairdner Dolerite|70826|6|Mentioned|p14 tbl 5|Tonian|Tonian|Musgrave and Rudall Provinces. Described as a dyke suite.|825 Ma|||||20-MAY-20
72709|Gairdner Dolerite|70839|5|Briefly described|p327,336,339|Tonian|Tonian|Geological province: Musgrave Province. NW-trending mafic dyke suite across northern South Australia into Musgrave region. Equivalent to Amata Dolerite.|827+\-6 Ma|||||
72709|Gairdner Dolerite|71037|5|Briefly described|p22-23 Fig.2, p27 Fig.6|Neoproterozoic|Neoproterozoic|SHRIMP U-Pb baddelyite age 827 +/- 6 Ma (Wingate et al., 1998). Shown as Willouran age [radiometric age equivalent to Tonian].|827 +/- 6 Ma.|||Shown as age equivalent to Backy Point Formation and younger than Pandurra Formation and older than Tapley Hill Formation.|Dolerite dykes.|
72709|Gairdner Dolerite|71129|4|Described|p1,15,17,35,103-106,184,207-208,225,227|Tonian|Tonian|Of Stuart Shelf. NW-trending dolerite dyke swarm; part of the Willouran Basic Province, which also includes the Wooltana, Cadlareena and Noranda volcanics, Wilangee Basalt and Little Broken Hill Gabbro, and Beda Basalt. Related to the Rodinian break-up (Zhao et al., 1994, Li et al., 1999, Wang et al., 2010). Basaltic volcanism interpreted to be result of mantle plume upwelling, causing doming in the continental lithosphere (Zhao et al., 1994). Contains tholeiitic, within-plate basaltic composition with commonly smooth LREE-enriched patterns and high initial ENd values; geochemically similar to high-Ti continental flood basalts. Geochemical analysis indicate derivation by large-scale decompression melting of a large heterogeneous asthenopheric mantle plume with no significant crustal contamination. Emplacement occurred immediately after Beda Basalt and Backy Point Formation deposition. Age contrained by SHRUMP U-Pb dating of zircons and baddelyite to 827+\-6 Ma (Wingate et al., 1998), supported by LA-ICPMS U-Pb of hydrothermal apatite and titanite from Olympic Dam samples, yielding ages of c. 820-825 Ma (Huang et al., 2016, Apukhtina et al., 2016).|827+\-6 Ma (SHRIMP U-Pb baddelyite)|||Equivalent to Amata Dolerite. Intrudes into Moonabie Formation or Wandearah Formation or Gluepot Granite or Broadview Schist or Gawler Range Volcanics.|Dolerite; porphyritic, variably contains plagioclase, clinopyroxene, titanomagnetite, lesser hornblende, biotite, small amounts of olivine. Commonly weathered to saprolite in outcrop.|
72709|Gairdner Dolerite|71130|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|SHRIMP U-Pb baddeleyite age.|827 +/- 6 Ma (Wingate et al., 1998).||||Dolerite dykes.|
72709|Gairdner Dolerite|71131|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|SHRIMP U-Pb baddeleyite age.|827 +/- 6 Ma (Wingate et al., 1998).||||Dolerite dykes.|
72709|Gairdner Dolerite|71169|6|Mentioned|p82|Tonian|Tonian||c. 825 Ma|||||
72709|Gairdner Dolerite|71235|6|Mentioned|p3-p5, p9|Neoproterozoic|Neoproterozoic|||||||
72709|Gairdner Dolerite|71236|6|Mentioned|p5, p28, p32|Tonian|Tonian|Believed to be the intrusive equivalent of the Beda Volcanics. Dykes which intrude the Cultana Subsuite are visible in magnetic imagery. |c. 827 +/- 6 Ma (Wingate et al., 1998)|||Intrudes the Cultana Subsuite.||16-MAR-23
72709|Gairdner Dolerite|71268|4|Described|GEOL_LUT_CSV files|Tonian|Tonian|Geological Province: Paterson Orogen. Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma). See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 100k_interpgeol_lut.csv, 100k_geologyl_lut.csv, 250k_interpgeol_lut.csv, 500k_interpgeol_lut.csv, 2_5m_interpdykel15_lut.csv.|827+\-6 Ma; 824+\-4 Ma||||Medium-grained dolerite and metadolerite; typically intergranular to subophitic; polygonal granoblastic where metamorphosed|
72709|Gairdner Dolerite|71317|6|Mentioned|p15|Neoproterozoic|Neoproterozoic|Gawler Craton.||||||
72709|Gairdner Dolerite|71321|5|Briefly described|p1,11,50,64|Tonian|Tonian|Geological province: Musgrave Province. Intruded post-c. 1085-1040 Ma Giles Event (p11 for references).|c. 820 Ma|||Correlable to Amata Dolerite (Musgrave Province).||
72709|Gairdner Dolerite|71413|6|Mentioned|p32 Fig 2|||Geological province: Gawler Craton. ||||||
72709|Gairdner Dolerite|71416|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Geochronology by Wingate et al. (1998).|827 +/- 6 Ma (SHRIMP U-Pb baddeleyite age).|||Correlative of Amata Dolerite.||
72709|Gairdner Dolerite|71712|5|Briefly described|p411, p419|Tonian|Tonian|Age based on Pb\Pb badeleyite geochron.|827 +\- 6 Ma Pb-Pb baddelyite age|||Intrudes the Pandurra Formation.  Coeval with Beda Basalt.||31-MAR-20
72709|Gairdner Dolerite|71859|6|Mentioned|p18|Neoproterozoic|Neoproterozoic|||||||
72709|Gairdner Dolerite|71862|6|Mentioned|p8, p12|Neoproterozoic|Neoproterozoic|||||||
72709|Gairdner Dolerite|71895|4|Described|p10, p25, p61-p63, APP1. p19,-p20|Neoproterozoic|Neoproterozoic|Also intrudes crystalline basement. Recognised in geophysics as long, sub-parallel, linear magnetic anomalies. This unit is the intrusive equivalent of the Beda Basalt. Spectral analysis is provided. App5. p110, p162, p164, APP8. p202 .Petrogaphic descriptions for numerous samples are provided in App5.|c. 800 Ma|||Intrudes the Pandurra Formation.|Dolerite and basaltic rocks.|
72709|Gairdner Dolerite|72089|6|Mentioned|p11|||Gawler Craton. Intersected in MSDP04.||||||
72709|Gairdner Dolerite|72090|5|Briefly described|p42, p44, p46|||Gawler Craton.|||||Grey, massive, fine- to coarse grained dolerite.|
72709|Gairdner Dolerite|72237|6|Mentioned|p29|Neoproterozoic|Neoproterozoic|Geological province: Gawler Craton.||||||
72709|Gairdner Dolerite|72238|5|Briefly described|p34,42-44|Tonian|Tonian|Geological province: Musgrave Province. Part of the Gairdner LIP, alongside Amata Dolerite, Willouran Basic province and other coeval mafic igneous rocks (see p34 for references). SHRIMP U-Pb age of 827+\-6 Ma from baddeleyite and zircon extracted from a dolerite dyke sample from drillhole RL 1 (Reedy Lagoon, northwestern Stuart Shelf, SA Geodata drillhole number 16695; Wingate et al. 1998). LA-ICPMS U-Pb age of c. 825-820 Ma of magmatic apatite and hydrothermal apatite and titanite at Olympic Dam (Huang et al. 2015, Apukhtina et al. 2016). Related to the first magmatic cycle (c. 825-800 Ma) in the South China Block.||||Equivalent to Amata Dolerite.||
72709|Gairdner Dolerite|72242|6|Mentioned|p27,29|Tonian|Tonian|Geological province: Coompana Province, Western Gawler Craton.||||||
72709|Gairdner Dolerite|72344|6|Mentioned|p3|||Coompana Province.||||||
72709|Gairdner Dolerite|72725|6|Mentioned|p25-30|Tonian|Tonian|Dyke swarm with NNW-SSE trending dykes. Appear sparse and distributed in the 1A Tallaringa North survey area. Is preferentially expressed in many of the magnetic field enhancement images because the top of the dykes are shallower than most other strong magnetisations.|c. 820-830 Ma|||Intrudes Callana Group.||
72709|Gairdner Dolerite|73061|6|Mentioned|p1069|Neoproterozoic|Neoproterozoic|Gairdner Dyke Swarm in text. Gawler Craton.|~827 Ma|||||
72709|Gairdner Dolerite|73091|6|Mentioned|map legend||||||||Dolerite dykes.|30-NOV-21
72709|Gairdner Dolerite|73103|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Is also shown in the Solid Geology Interpretation map, below the main Whyalla 250k map. Sm-Nd ages of 867 +/- 47 Ma and 802 +/- 35 Ma are also given.|827 +/- 6 Ma (U-Pb).||||Dolerite dykes locally intruded by black porphyritic basalt.|
72709|Gairdner Dolerite|73110|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Other age determinations given are 867 +/- 47 Ma (Sm-Nd), and 802 +/- 35 Ma (Sm-Nd).|827 +/- 6 Ma (U-Pb).||||Dolerite dykes locally intruded by black porphyritic basalt.|
72709|Gairdner Dolerite|73166|6|Mentioned|p644|Neoproterozoic|Neoproterozoic|Gawler Craton. Intrudes the Olympic Cu-Au Province.|0.83 Ga|||||
72709|Gairdner Dolerite|73188|6|Mentioned|p315|Tonian|Tonian|Geochron from Wingate et al. (1998). Accompanied earliest rifting in the Adelaide Geosyncline.|827 +/- 6 Ma|||||
72709|Gairdner Dolerite|73225|5|Briefly described|p5|||NW-trending dykes.|c.825 Ma.|||||
72709|Gairdner Dolerite|73227|6|Mentioned|p24|Tonian|Tonian|Geochron from Wingate et al. (1998). Interpreted as feeders for the Beda Basalt.|827 +/- 6 Ma|||Equivalent to Beda Basalt. Intrudes Pandurra Formation.||
72709|Gairdner Dolerite|73234|6|Mentioned|p6|Tonian|Tonian|Contemporaneous with Beda Basalt.|c. 825 Ma|||||
72709|Gairdner Dolerite|73235|6|Mentioned|p53|Tonian|Tonian||c. 825 Ma|||||
72709|Gairdner Dolerite|74361|6|Mentioned|p164, 177|Neoproterozoic|Neoproterozoic|Intrudes the northern and eastern Gawler Craton.|c.830 Ma.||||Mafic dykes.|
72709|Gairdner Dolerite|74367|5|Briefly described|p8, p18|Tonian|Tonian|Suggested to be coeval with Noranda Volcanics, Cadlareena Volcanics, Beda Basalt, Willangee Basalt and the 'Depot Creek Volcanics'. Correlation with Boucaut Volcanics has proven to be incorrect.|827+/-6 Ma|||Correlated with Wooltana Volcanics||
29850|Gantheaume Sand Member|60953|5|Briefly described|Map Legend|Holocene|Holocene|White calcareous and siliceous coastal dune sand.||||||
29850|Gantheaume Sand Member|60958|5|Briefly described|Map Legend|Holocene|Holocene|Of the Saint Kilda Formation. Unconsolidated aeolian cliff-top dunes and sand spreads. Originates from aeolian reworking of the Bridgewater Formation.||||||14-APR-05
29850|Gantheaume Sand Member|61108|5|Briefly described|map legend|Holocene|Holocene|White calcareous and siliceous coastal dune sand.||||||
29850|Gantheaume Sand Member|61121|5|Briefly described|Map legend|Holocene|Holocene|Of the Saint Kilda Formation. Unconsolidated aeolian cliff-top dunes and sand spreads; originates from aeolian reworking of Bridgewater Formation, particularly out of receding coastal cliffs.||||||07-JUN-05
29850|Gantheaume Sand Member|64282|5|Briefly described|Map legend|Holocene|Holocene|Of the Saint Kilda Formation. Unconsolidated aeolian cliff-top dunes and sand spreads. Originates from aeolian reworking of Bridgewater Formation particluarly out of receding coastal cliffs.||||||19-JUN-08
29850|Gantheaume Sand Member|65375|5|Briefly described|p42.|Holocene|Holocene|||Unit in Saint Kilda Formation.|||Aeolian cliff top dunes, particularly formed from receding coastal cliffs.|
29850|Gantheaume Sand Member|65921|6|Mentioned|p2 (map legend)|Quaternary|Quaternary|||||||
29850|Gantheaume Sand Member|68131|6|Mentioned|p7, p17|Holocene|Holocene|Yorke Peninsula.||||||
29850|Gantheaume Sand Member|70382|5|Briefly described|p29 Fig 3|Holocene|Holocene|Yorke Peninsula region.|||||Unconsolidated aeolian cliff top dunes and sands|
29850|Gantheaume Sand Member|73107|5|Briefly described|Map legend.|Holocene|Holocene|Originates from aeolian reworking of Bridgewater Formation, particularly out of receding coastal cliffs.|||||Unconsolidated aeolian cliff-top dunes and sand spreads.|
25918|Garford Formation|22587|6|Mentioned|p79 Fig.7|Middle Miocene|Early Miocene|||||||
25918|Garford Formation|22613|4|Described|p23|Miocene|Miocene|||||||
25918|Garford Formation|22614|5|Briefly described|map|Pliocene|Miocene|||||||
25918|Garford Formation|22916|5|Briefly described|12|||||||||
25918|Garford Formation|22938|6|Mentioned|p236|||||||||
25918|Garford Formation|23343|5|Briefly described|39|Miocene|Miocene|||||||
25918|Garford Formation|23479|5|Briefly described|p26|Neogene|Neogene|In palaeochannels incised into Eromanga Basin sediments||||||04-NOV-10
25918|Garford Formation|24358|5|Briefly described|p32|Early Pliocene|Late Miocene|Geological Province: Eucla Basin.||||||17-MAR-05
25918|Garford Formation|24396|4|Described|p216, p218 Fig.3|Early Pliocene|Middle Miocene|Lacustrine calcareous clays/carbonates. Contains the Kingoonya Member. See also p220 Fig.4, p222 Fig.5. Overlying the Gawler Craton.||||||04-NOV-10
25918|Garford Formation|24606|5|Briefly described|p956, p958 Fig. 3|Early Pliocene|Middle Miocene|Overlain by the Narlaby Formation. Geological Province: Eucla Basin.||||||
25918|Garford Formation|35080|2|Defined|p8|middle Tertiary|middle Tertiary|||||||
25918|Garford Formation|36244|6|Mentioned|p2|||Refers Benbow & Pitt 1978 for a definition.||||||
25918|Garford Formation|36966|6|Mentioned|p86|||||||||
25918|Garford Formation|37852|6|Mentioned|Fig.3|||||||||
25918|Garford Formation|38604|6|Mentioned|Map legend|Miocene|Miocene|||||||
25918|Garford Formation|38605|4|Described|p29|||See also Table 5.||||||
25918|Garford Formation|40912|6|Mentioned|Map legend|Pliocene|Miocene|Miocene-Pliocene||||||
25918|Garford Formation|41619|6|Mentioned|Map legend|Tertiary||||||||
25918|Garford Formation|42356|4|Described|Microfiche 7pp18|Miocene||See also DESC p18, Fig15 P119 Microfiche 7 p15, Fig.4, Fig.9, 10, 12, 13.||||||16-APR-18
25918|Garford Formation|42465|5|Briefly described|Map Legend|||||||||
25918|Garford Formation|42466|5|Briefly described|Map Legend|||||||||
25918|Garford Formation|42469|5|Briefly described|p39, p46|||||||||
25918|Garford Formation|42475|3|Fully described|p21|||||||||
25918|Garford Formation|42546|5|Briefly described|Map legend|Tertiary||||||||
25918|Garford Formation|42736|5|Briefly described|map legend|Tertiary||||||||
25918|Garford Formation|42816|3|Fully described|p24|||||||||
25918|Garford Formation|43053|5|Briefly described|Map Legend|Pliocene|Miocene|Lacustrine dolomite, clay, sand and silt. Geological Province: Eucla Basin palaeodrainage.||||||25-MAY-05
25918|Garford Formation|43258|5|Briefly described|Map Legend|Pliocene|Miocene|||||||
25918|Garford Formation|43298|6|Mentioned|Map Legend|Pliocene|Miocene|||||||
25918|Garford Formation|43686|6|Mentioned|p236|||||||||
25918|Garford Formation|44133|5|Briefly described|p185, 180 Fig. 10.22|Pliocene|Pliocene|Geological Province: Eucla Basin. Thickness: 20m. Underlies: Narlaby Formation.||||||
25918|Garford Formation|44695|5|Briefly described|Map Legend|Pliocene|Miocene|||||||
25918|Garford Formation|44935|5|Briefly described|Map Legend||Pliocene|||||||
25918|Garford Formation|60497|5|Briefly described|p42|Early Pliocene|Middle Miocene|Includes the Kingoonya Member.  Geological Province: Eucla Basin.||||||
25918|Garford Formation|60953|5|Briefly described|Map Legend|Pliocene|Miocene|Lacustrine dolomite, clay, sand and silt. Geological Province: Eucla Basin. Paleodrainage.||||||27-APR-05
25918|Garford Formation|61108|5|Briefly described|map legend|Pliocene|Miocene|Lacustrine dolomite, clay, sand and silt. Geological Province: Eucla Basin palaeodrainage.||||||
25918|Garford Formation|61155|5|Briefly described|p17|Early Pliocene|Early Miocene|Age: 18.5-14.5Ma; and, 5.5-4.0Ma. Max. thickness for older section: 70m. Geological Province: Eucla Basin; also in the Oodnadatta area||||||
25918|Garford Formation|61234|4|Described|p6, p7 Fig 4.|Early Pliocene|Middle Miocene|Geological Province: Eucla Basin. Overlies Khasta Formation unconformably. Lacustrine mudstone and dolomitic limestone.||||||14-MAY-07
25918|Garford Formation|61814|5|Briefly described|p26|Miocene|Miocene|Predominantly lacustrine clays. Geological Province: Gawler Craton.||||||08-FEB-10
25918|Garford Formation|61839|5|Briefly described|p227|Miocene|Eocene|Predominantly lacustrine clays. Overlying Gawler Craton.||||||04-NOV-10
25918|Garford Formation|64646|6|Mentioned|p23 Fig. 3, p24 Fig. 4|Pliocene|Middle Miocene|Includes Kingoonya Member. In palaeovalleys overlying Gawler Craton.||||||04-NOV-10
25918|Garford Formation|65194|5|Briefly described|p163-164, p171-172|Early Pliocene|Middle Miocene|Tallaringa and Garford palaeovalleys. Includes Kingoonya Member. Predominantly alkaline lacustrine and flood-plain deposits: very fine to coarse sand and silt, grading upwards into clay, dolomitic clay and dolomite. Associated with uranium mineralisation. Overlies Pidinga Formation unconformably.||||||11-APR-16
25918|Garford Formation|65385|4|Described|pS127, pS129 Fig.3|Late Eocene|Late Eocene|Unconformably overlies Pidinga Formation. Unconformably overlain by chalcedonic limestone. Consists of dolomitic clays, clayey sands and dolomitic limestones. Marginal marine to estuarine facies sediments representing a marine transgression.||||||08-MAR-12
25918|Garford Formation|65922|5|Briefly described|p25 Tb. 4, p26|Pliocene|Miocene|Khaki to greenish grey to brown, well-laminated to locally flaggy clay, silt and sand. Derived from Hutchison Group and locally, Gawler Range Volcanics and Hiltaba Suite. Overlies either Pidinga Formation or weathered basement. ||||||
25918|Garford Formation|67462|5|Briefly described|Map legend.|Neogene|Neogene|Eucla Basin; Gawler Craton. Shown as two seperate intervals, one middle Miocene, the other Late Miocene to Piocene.|||Includes Kingoonya Member.|||05-DEC-13
25918|Garford Formation|67921|5|Briefly described|Map legend|Pliocene|Miocene|||||Equivalent to Mangatitja Formation.|Lacustrine deposits of chalcedonic limestone and grey, green or red clayey sand to sandy clay.|
25918|Garford Formation|68128|5|Briefly described|p27, p43, p64, p71, p77|Pliocene|Eocene|Gawler Craton. Deposited in a lacustrine environment.|||||Mudstone, carbonate, minor sandstone.|31-JAN-23
25918|Garford Formation|68715|6|Mentioned|p30 Fig.5|Zanclean|Burdigalian|SW and NW Gawler Craton, Eucla Basin.||||||
25918|Garford Formation|69004|4|Described|iii,  p19, p28-p29, p32, p34-p35, p38|Miocene|Miocene|Eucla Basin. Alkaline lake deposits are common.|||Includes the Kingoonya Member.|Unconformably overlies the Pidinga Formation.|Oxidised sands, lacustrine calcareous clays and carbonates.|
25918|Garford Formation|69598|6|Mentioned|p9|Early Pliocene|Middle Miocene||||Includes the Kingoonya Member.|Overlain by the Narlaby Formation.||
25918|Garford Formation|69648|4|Described|p4, p6 Fig.3, p27-28, p32, map legend|Pliocene|Miocene|Tietkins Plain. Immature karst. Originally defined from Garford Palaeochannel on COOBER PEDY. Best exposures at Roadside Quarry and in two Tietkins wells nearby. Max thickness: likely <15 m. In lower part of formation (intersected in drillholes) locally ooid-rich mudstones, packstones and grainstone occur. Exact age arguable due to lack of diagnostic fossils.||Immarna Group||Unconformably overlies Hampton Sandstone and Pidinga Formation; overlain by Ilkina Formation.|Alkali, playa lake carbonates; lacustrine, argillaceous muds, carbonate mudstones; on OOLDEA dominantly calcareous/dolomitic mudstones and dolomite, palygorskite-rich argillaceous muds can occur near base; very little terrigenous clastic components.|
25918|Garford Formation|69649|5|Briefly described|p31-32, p48|Eocene|Eocene|Eucla Basin. Up to 100m thick. Lacustrine, flood-plain, lagoonal swamp and locally evaporative environments. Associated with sub-economic U mineralisation near contact with Pidinga Formation.||||Locally unconformably overlies Pidinga Formation.|Succession of oxidised, grey, green and cream, to black mud, minor carbonate and local basal and interbedded carbonaceous sand and grit.|
25918|Garford Formation|70397|5|Briefly described|p3|Middle Miocene|Middle Miocene|Eucla Basin. Equivalent stratigraphic level to Colville Sandstone and Nullabor Limestone.||Unit of Eucla Group.||Underlain by Wilson Bluff Limestone.||
25918|Garford Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||mudstone|
25918|Garford Formation|71317|4|Described|p137, p143-p144|Middle Miocene|Middle Miocene|Eucla Basin. Between 10 and 60m thick in places (not on Peltabinna). Deposited as lacustrine clay and fluviatile sand.||||Overlies the Pidinga Formation. Overlain by the Moornaba Sand. Equivalent to the Namba and Etadunna Formations.|Mudstone and minor horizons of silt and fine- to coarse-grained sand.|
25918|Garford Formation|71361|5|Briefly described|p5, p18|Middle Miocene|Early Miocene|Eucla Basin. Deposited in a lacustrine environment.||||||
25918|Garford Formation|71559|5|Briefly described|p19|Pleistocene|Miocene|Geological province: Gawler Craton.|||||Mudstone, carbonate, stomatolitic, oncolytic and oolitic, gastrapods, minor sandstone horizons. Upward change from argillaceous to carbonate mudstone. Lacustrine.|
25918|Garford Formation|71560|5|Briefly described|Map legend.|Pleistocene|Miocene|Lacustrine deposits.||Immarna Group.|||Mudstone, carbonate, stromatolitic, oncolytic and oolitic, gastropods, minor sandstone horizons. Upward change from argillaceous to carbonate mudstone.|
25918|Garford Formation|73099|5|Briefly described|Map legend.|Pliocene|Pliocene|Meramangye and Tallaringa Palaeochannels.||Immarna Group.||Overlies Pidinga Formation (Burdunga Subgroup).|Limestone and grey-green clayey sandstone and sandy claystone. Nodular, sheet and rubbly calcrete duricrust developed in palaeochannels.|
25918|Garford Formation|73100|5|Briefly described|Map legend|Pliocene|Miocene|||||Equivalent to Mangatitja Formation.|Lacustrine deposits of chalcedonic limestone and grey, green or red clayey sand to sandy clay.|
25918|Garford Formation|73108|5|Briefly described|Map legend.|Pleistocene|Eocene||||||Mudstone, carbonate, stromatolitic, oncolitic and oolitic, gastropods, minor sandstone horizons. Upward change from argillaceous to carbonate mudstone. Lacustrine.|
25918|Garford Formation|73109|5|Briefly described|Map legend.|Pliocene|Miocene|Subcrop and minor outcrop.||||Equivalent to Mangatitja Formation.|Lacustrine deposits of chalcedonic limestone and grey, green or red clayey sand to sandy clay. Calcareous regolith on top.|
25918|Garford Formation|73111|5|Briefly described|Map legend.|Pliocene|Miocene|Subcrop and minor outcrop.||||Equivalent to Mangatitja Formation.|Lacustrine deposits of chalcedonic limestone and grey, green or red clayey sand to sandy clay. Calcareous regolith on surface.|
25918|Garford Formation|73232|5|Briefly described|p8, p10|Pliocene|Miocene|Lacustrine palaeovalley infill. Well known from palaeovalleys along the Eucla Basin northern margin. One of the main stratigraphic units in palaeovalleys that trend southwards from the Musgrave Province across the Officer Basin to the Eucla Basin. [Approximately 58 m of mudstone and sandstone in drillhole DH1a from the Lindsay East Palaeovalley is attributed to this unit in Fig. 5 but not explicitly discussed in the text].|||||May include brown-black organic-, sulfidic- and clay-rich basal muds, olive-green muds, massive gypsum, and partly massive, moderately sorted, fine- to coarse-grained, quartz-rich sands and sandstones with intercalations of clay and gravel.|
40399|Gawler Range Volcanics, Lower|24197|6|Mentioned|p30, p31|||Informal - see Gawler Range Volcanics. This is a Roxby Downs-type of the Hiltaba Suite. Underlies Upper Gawler Range Volcanics.||||||07-FEB-11
40399|Gawler Range Volcanics, Lower|24422|6|Mentioned|p84 Fig. 1|Mesoproterozoic|Mesoproterozoic|Geological Province: Gawler Craton. Informal - see the Gawler Range Volcanics.||||||
40399|Gawler Range Volcanics, Lower|24505|5|Briefly described|p5 Fig. 1|||Informal - see Gawler Range Volcanics. Geological Province: Gawler Craton.||||||
40399|Gawler Range Volcanics, Lower|50605|5|Briefly described|P(ii)|Mesoproterozoic|Mesoproterozoic|Geological Province: Gawler Craton & Curnamona Province. Of the Hiltaba Supersuite.||||||30-AUG-04
40399|Gawler Range Volcanics, Lower|60515|5|Briefly described|p116 Fig.1, p117||||c.1590 Ma.||||Basalt, andesite and rhyolite.|
40399|Gawler Range Volcanics, Lower|60953|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|||||||
40399|Gawler Range Volcanics, Lower|60954|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Geological Province: Gawler Craton.||||||31-MAY-05
40399|Gawler Range Volcanics, Lower|61108|5|Briefly described|map legend|Mesoproterozoic|Mesoproterozoic|Age: 1592-1589 Ma. Younger succession includes Nonning Rhyodacite and Eucarro Dacite: dacite to rhyolite, minor andesite and basalt. Older succession includes Roopena Volcanics: basalt, andesite, rhyodacite and rhyolite.||||||23-JUN-05
40399|Gawler Range Volcanics, Lower|61522|5|Briefly described|p5 Fig.1|||Geological Province: Gawler Craton.||||||02-JUN-06
40399|Gawler Range Volcanics, Lower|63275|5|Briefly described|p14 Fig.1.|Early Mesoproterozoic|Early Mesoproterozoic|See references to Gawler Range Volcanics throughout the article.||||||
40399|Gawler Range Volcanics, Lower|66302|5|Briefly described|p4Fig.3, p5 Fig.4, p6, p41, p42|||Gawler Range Volcanics Domain.|||||Dacite-rhyodacite-rhyolite ignimbrites and flows with thick interlayered successions of basaltic lavas.|
40399|Gawler Range Volcanics, Lower|67112|6|Mentioned|p3 Fig.2|Mesoproterozoic|Mesoproterozoic|Gawler Craton.||||||
40399|Gawler Range Volcanics, Lower|67900|5|Briefly described|p19-20, 30-31, 33|Mesoproterozoic|Mesoproterozoic|Blissett et al. (1993). Gawler Craton. After the first mention, appears as lower GRV. At least three discrete volcanic centres: Kokatha (Chitanilga Volcanic Complex); Lake Everard (Glyde Hill Volcanic Complex); and Roopena (Roopena Volcanics).|||Chitanilga Volcanic Complex, Glyde Hill Volcanic Complex, Roopena Volcanics, Waganny Dacite.||A developmental phase of bimodal mafic and felsic volcanic rocks, ranging through basalt, andesite, dacite, rhyodacite and rhyolite.|
40399|Gawler Range Volcanics, Lower|68158|6|Mentioned|p4|||||Gawler Range Volcanics.||||
40399|Gawler Range Volcanics, Lower|69649|6|Mentioned|p6 Fig.4, p16|Mesoproterozoic|Mesoproterozoic||1592 +/- 3 Ma. U-Pb zircon: Fanning et al. (1988).|||||
40399|Gawler Range Volcanics, Lower|69666|6|Mentioned|p27 Fig.3|Mesoproterozoic|Mesoproterozoic|||||||
40399|Gawler Range Volcanics, Lower|70502|6|Mentioned|p17||||1.59 Ga.|||Intrudes Roxby Downs Granite and Olympic Dam Breccia Complex.||
40399|Gawler Range Volcanics, Lower|70659|5|Briefly described|p3, p5-6, p36-37, p47-48|Mesoproterozoic|Mesoproterozoic|See also Gawler Range Volcanics (p1-14, p36-37, p42-43, p47-49, p57-59).|||Ealbara Rhyolite and Konkaby Basalt; Chitanilga Volcanic Complex; Glyde Hill Volcanic Complex; Bittali Rhyolite and Waganny Dacite; Roopena Basalt, Fresh Well Formation and Angle Dam Volcanics; et al.||Five recognised volcanic successions, including dacite to rhyolite, ignimbrites and tuffs with minor basalt erupted from discrete volcanic centres.|06-FEB-17
40399|Gawler Range Volcanics, Lower|71037|5|Briefly described|p21 Fig.1, p22-23 Fig.2, p24, p25 Fig.4|Mesoproterozoic|Mesoproterozoic|Bimodal volcanics. Shown as Lower Gawler Range Volcanics (GRV). See also p26 Fig.5, p27 Fig.6.|c.1591 (CA-TIMS)||Includes Spearfelt Rhyodacite, Roopena Basalt, Fresh Well Formation, Angle Dam Volcanics, and 4 unnamed subunits.|Shown as younger than Moola Suite and older than Gawler Range Volcanics (Upper).|Includes rhyodacite, red-brown, porphyritic, phenocrysts of feldspar, pyroxene, hornblende and lesser quartz. Arkosic and lithic sandstone, siltstone, dolomitic mudstone, pebble conglomerate. Rhyolitic to dacitic lava, ignimbrite and lapillistone.|
40399|Gawler Range Volcanics, Lower|71129|4|Described|p17,35,47-51,53-56,66,78,89|Calymmian|Calymmian|Geological Province: Gawler Craton. Abbreviated as lower GRV in text. Volcanic centres are interpreted to be derived from fractional crystallisation and crustal contamination of mantle melts (Giles, 1988, Stewart, 1994, Creaser, 1995, Fricke, 2005). Intersected by MSDP01 (drillhole 287995), intersecting reddish-brown, massive, evenly porphyritic rhyolite (964.2-EOH 1116.8m), interpreted to be part of a subaerial etrusive-effusive felsic volcanic sequence. Plagioclase phyric basaltic lava flows intersected in MSDP01 (665.15-964.2) and MSDP04 (340-437.2m) are interpreted to be extruded into shallow, subaqueous environments, coming into contact with waters bodies in sites of active fluvial-deltaic sedimentation. Age contrained by underlying Spearfelt Rhyodacite (1591.2+\-0.5 Ma (U-Pb CA-TIMS). See also p95,105,183-184,189,207-208,225,227.|c. 1591 Ma (max dep)||Includes Fresh Well Formation, Roopena Basalt, Angle Dam Volcanics and Spearfelt Rhyodacite.|Underlain unconformably by Broadview Schist.|Rhyolitic to dacitic lavas, ignimbrites and tuffs with minor basaltic lavas erupted from discrete volcanic centres.|
40399|Gawler Range Volcanics, Lower|71130|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic||||Angle Dam Volcanics, Fresh Well Formation, Roopena Basalt, Spearfelt Rhyolite.||Felsic, intermediate and mafic volcanics; rhyolitic to dacitic lava, ignimbrite, minor tuff, lapillistone and tuffaceous mudstone.|
40399|Gawler Range Volcanics, Lower|71131|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic||||Angle Dam Volcanics, Fresh Well Formation, Roopena Basalt, Spearfelt Rhyolite.||Felsic, intermediate and mafic volcanics; rhyolitic to dacitic lava, ignimbrite, minor tuff, lapillistone and tuffaceous mudstone.|
40399|Gawler Range Volcanics, Lower|71317|6|Mentioned|p15|Mesoproterozoic|Mesoproterozoic|Gawler Craton.||||||
40399|Gawler Range Volcanics, Lower|71322|6|Mentioned|p103, p136|Mesoproterozoic|Mesoproterozoic|Northern Eyre Peninsula.||||||
40399|Gawler Range Volcanics, Lower|71559|6|Mentioned|p19-20|Mesoproterozoic|Mesoproterozoic|See also Gawler Range Volcanics.|||Includes Bittali Rhyolite.|||19-JUN-19
40399|Gawler Range Volcanics, Lower|71560|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic||||Bittali Rhyolite.|||
40399|Gawler Range Volcanics, Lower|71859|5|Briefly described|p3|Mesoproterozoic|Mesoproterozoic|Nuyts Domain, southern Gawler Craton.||||||
40399|Gawler Range Volcanics, Lower|72058|6|Mentioned|p171|||Middleback Ranges, Gawler Craton.|~1597 to 1589 Ma |||||
40399|Gawler Range Volcanics, Lower|72065|5|Briefly described|p105,111|Calymmian|Calymmian|Geological province: Gawler Craton. Thickness: 0.5-0.3km thick. Described as the "developmental' phase of the GRV evolutionary sequence, with small to moderate volume, and gently to moderately dipping units. Within the exposed Lower GRV, rhyolitic and dacitic lavas, ignimbrites and minor volcaniclastic rocks are far more abundant than tholeiitic basalt and basaltic andesite lavas (Agangi, 2011; Allen et al., 2008; Curtis et al., 2018).||||||
40399|Gawler Range Volcanics, Lower|72090|5|Briefly described|p11-p14|||Gawler Craton. Referred to as the Lower GRV throughout the text.|||Includes the Ealbara Rhyolite, Konkaby Basalt, Mentor Formation, Lake Gairdner Rhyolite, Waganny Dacite, Bittali Rhyolite, Roopena Basalt, Angle Dam Volcanics and Fresh Well Formation.|||
40399|Gawler Range Volcanics, Lower|73026|6|Mentioned|p4 fig1.2, p9|Mesoproterozoic|Mesoproterozoic||c. 1593 Ma|||||
40399|Gawler Range Volcanics, Lower|73110|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic||||Ealbara, Lake Gairdner, Bittali Rhyolites; Konkaby, Roopena Basalts; Chitanilga, Glyde Hill, Volcanic Complexes; Waganny Dacite; Angle Dam Volcanics.||Basalt to rhyolite lava, ignimbrite and tuff.|
40399|Gawler Range Volcanics, Lower|73263|6|Mentioned|p591-592|Calymmian|Calymmian|Geochron from Jagodzinski et al. (2016). Contemporaneous with high-sulfidation epithermal silver and porphyry copper-gold mineralisation.|ca 1591-1589 Ma|||||
40400|Gawler Range Volcanics, Upper|24197|6|Mentioned|p30-31|||Informal - see Gawler Range Volcanics. This is comagmatic with the Kokatha type of the Hiltaba Suite. Comprises flat-lying sheets of massive porphyritic dacite and rhyodacite. Overlies Lower Gawler Range Volcanics.||||||07-FEB-11
40400|Gawler Range Volcanics, Upper|24422|6|Mentioned|p84 Fig. 1|Mesoproterozoic|Mesoproterozoic|Geological Province: Gawler Craton. Informal - see the Gawler Range Volcanics.||||||
40400|Gawler Range Volcanics, Upper|24505|5|Briefly described|p5 Fig. 1|||Informal - see Gawler Range Volcanics. Geological Province: Gawler Craton.||||||
40400|Gawler Range Volcanics, Upper|50605|5|Briefly described|p(ii)|Mesoproterozoic|Mesoproterozoic|Geological Province: Gawler Craton & Curnamona Province. Of the Hiltaba Supersuite.||||||
40400|Gawler Range Volcanics, Upper|60515|6|Mentioned|p116 Fig.1 ||||c1590|||||
40400|Gawler Range Volcanics, Upper|60953|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|||||||
40400|Gawler Range Volcanics, Upper|60954|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Geological Province: Gawler Craton.||||||31-MAY-05
40400|Gawler Range Volcanics, Upper|61108|5|Briefly described|map legend|Mesoproterozoic|Mesoproterozoic|Includes Yardea Dacite. Dacite and rhyodacite. Age: 1592 Ma.||||||23-JUN-05
40400|Gawler Range Volcanics, Upper|61522|5|Briefly described|p5 Fig.1|||Geological Province: Gawler Craton.||||||
40400|Gawler Range Volcanics, Upper|63275|5|Briefly described|p14 Fig.1.|Early Mesoproterozoic|Early Mesoproterozoic|See references to Gawler Range Volcanics throughout the article.||||||
40400|Gawler Range Volcanics, Upper|66302|5|Briefly described|p4Fig.3, p5 Fig.4, p6, p42|||Gawler Range Volcanics Domain.|||||Thick, porphyritic dacite sheets that are predominantly ignimbritic.|
40400|Gawler Range Volcanics, Upper|67112|6|Mentioned|p3 Fig.2|Mesoproterozoic|Mesoproterozoic|Gawler Craton.||||||
40400|Gawler Range Volcanics, Upper|67900|5|Briefly described|p19-20, 30, 33|Mesoproterozoic|Mesoproterozoic|Blissett et al. (1993). Gawler Craton. After the first mention, appears as upper GRV. Up to ~1.5km thick.|||Yardea Dacite.||Extensive, flat-lying, relatively undeformed felsic (rhyolite-rhyodacite-dacite) volcanic rocks.|
40400|Gawler Range Volcanics, Upper|69649|6|Mentioned|p6 Fig.4, p16|Mesoproterozoic|Mesoproterozoic||1591 +/- 3 Ma. U-Pb zircon: Fanning et al. (1988).|||||
40400|Gawler Range Volcanics, Upper|70659|5|Briefly described|p3, p5-6, p8|Mesoproterozoic|Mesoproterozoic|See also Gawler Range Volcanics (p1-14, p36-37, p42-43, p47-49, p57-59).|||Carnding Rhyodacite, Chandabooka Dacite, Yardea Dacite.||Consists of three regionally extensive, thick (200-300m), high-T (900-1100 degrees C) felsic lava flows.|06-FEB-17
40400|Gawler Range Volcanics, Upper|71037|5|Briefly described|p21 Fig.1, p22-23 Fig.2, p24, p26 Fig.5|Mesoproterozoic|Mesoproterozoic|Shown as Upper Gawler Range Volcanics.|||Includes Eucarro Rhyolite, in this area.|||
40400|Gawler Range Volcanics, Upper|71129|5|Briefly described|p17,47,184,190,225,227|Calymmian|Calymmian|Geological Province: Gawler Craton. Abbreviated as upper GRV in text. Consists of three regionally extensive thick (200-300 m) high temperature (900-1100C) felsic lava flows; isotopically homogenous and define a single fractionation trend, suggesting that they were derived from the periodic tapping of a single stratified magma reservoir (Stewart, 1994).|||Includes Eucarro Rhyolite.||Felsic lava flows.|
40400|Gawler Range Volcanics, Upper|71130|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic||||Eucarro Rhyolite.|||
40400|Gawler Range Volcanics, Upper|71131|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic||||Eucarro Rhyolite.|||
40400|Gawler Range Volcanics, Upper|71317|6|Mentioned|p15|Mesoproterozoic|Mesoproterozoic|Gawler Craton.||||||
40400|Gawler Range Volcanics, Upper|71322|6|Mentioned|p103, p136|Mesoproterozoic|Mesoproterozoic|Northern Eyre Peninsula.||||||
40400|Gawler Range Volcanics, Upper|71559|5|Briefly described|p19-20, p23, p26|Mesoproterozoic|Mesoproterozoic|Geological province: Gawler Craton. See also Gawler Range Volcanics. Abbreviated to upper GRV in text. Affected by brittle faulting along NW-trending Progress-Eurilla FZ (Werner et al., 2017c). Shown as upper GRV p23, 26.|||Includes Yardea Dacite, Mount Friday Formation, Paney Rhyolite Member, Yannabie Rhyolite, Eucarro Rhyolite.|||19-JUN-19
40400|Gawler Range Volcanics, Upper|71560|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic||||Eucarro Rhyolite, Mount Friday Formation, Yardea Dacite.||Rhyolite, dacite.|
40400|Gawler Range Volcanics, Upper|71859|5|Briefly described|p3|Mesoproterozoic|Mesoproterozoic|Nuyts Domain, southern Gawler Craton.||||||
40400|Gawler Range Volcanics, Upper|72065|5|Briefly described|p105-106,108-109,111-112,114-120|Calymmian|Calymmian|Geological province: Gawler Craton. Described as the "mature" phase of the GRV evolutionary sequence, with extensive, gently dipping to flat-lying younger units. Contains a crystal cluster known as GRV-type crystal clusters: pyroxene and Fe-Ti oxides+\-apatite+\-zircon+\-plagioclase. Parental melt was likely hot, dry, and relatively reduced, as pyroxenes predominate over biotite. Interpreted that crystals formed within the magmatic system, and required a subsequent event or rejuvenation (magma recharge: increased temperature or melt volatile content for example) to free the crystal clusters prior to, and during extrusive unit emplacement.||||||
40400|Gawler Range Volcanics, Upper|72090|5|Briefly described|p11-p13|||Gawler Craton. Referred to as the Upper GRV throughout the text.|||Includes the Eucarro Rhyolite, Yardea Dacite, Mount Double Ignimbrite, Chandabooka Dacite and the Carnding Rhyodacite.|||
40400|Gawler Range Volcanics, Upper|73026|6|Mentioned|p4 fig1.2,|Mesoproterozoic|Mesoproterozoic||c. 1595-1570 Ma|||||
40400|Gawler Range Volcanics, Upper|73263|6|Mentioned|p592|||||||||
81055|Gawler Range Volcanics, lower|67909|4|Described|p124-129, 132, 134-138, 140-141|Mesoproterozoic|Mesoproterozoic|Eruption from distinct centres. Simplified logs. Volcanic textures and emplacement mechanisms of constituents tabulated. Photographs.|1592-1591 Ma.|Gawler Range Volcanics.|Chitanilga, Glyde Hill, Volcanic Complexes.|Is cut by Moonamby Dyke Suite.|Comprises thick (up to 3km) sequences of porphyritic dacite and rhyolite, interbedded with ignimbrites and minor mafic and intermediate lavas (basalt and basaltic andesite).|
81055|Gawler Range Volcanics, lower|70334|5|Briefly described|p12,75|Calymmian|Calymmian|Geological province: Gawler Craton. Mixed sequence of mafic and felsic volcanics; mafic rocks range in composition from basalt to andesite, and felsic rocks range from ryolite to dacite. Occurs in the Lake Everard area (Glyde Hill Complex) and Kokatha station area (Chitanilga Volcanic Complex) (GAIRDNER), Roopena station area (Roopena Volcanics) and Nonning area (southern GRV) (western PORT AUGUSTA), and in the Stuart Shelf and TARCOOLA-KINGOONYA areas. ||||||
81055|Gawler Range Volcanics, lower|70816|4|Described|p1,4-5, p8, 17-18|||Geological province: Gawler Ranges. Include bimodal mafic and felsic volcanic successions, such as those at Tarcoola and Roopena, felsic volcanic successions, such as that along the southern margin of the Gawler Ranges, as well as mafic-intermediate-felsic successions, such as the Chitanilga and Glyde Hill volcanic complexes.|||Includes Ealbara Rhyolite, Konkaby Basalt, Chitanilga Volcanic Complex, Glyde Hill Volcanic Complex, Bittali Rhyolite, Waganny Dacite, Roopena Basalt, Fresh Well Formation and Angle Dam Volcanics.||Felsic and mafic lavas, ignimbrites and tuffs erupted from discrete volcanic centres|30-MAY-19
81055|Gawler Range Volcanics, lower|70948|5|Briefly described|p973,975, 977-979, 984, 985|||Geological province: Gawler Craton. Where exposed along the SE margin of Gawler Ranges,  interlayered with volcanoclastic lacustrine sediments (Fresh Well Formation) and rhyolitic to dacitic lavas (Angle Dam Volcanics).|||||felsic and mafic lavas, ignimbrites and tuffs erupted from discrete volcanic centres|
81055|Gawler Range Volcanics, lower|72089|4|Described|p1-p2, p12-p13, p15, p24, p27|Mesoproterozoic|Mesoproterozoic|Gawler Craton. Intersected in three drillholes; MSDP01, MSDO03, MSDP04. Informally subdivided into unnamed units in drillholes. Intruded by an unnamed "flow-banded felsic unit" in drillhole MSDP04.|c. 1595-1587 Ma (Jagodzinski et al, 2016)||Includes the Roopena Basalt, Fresh Well Formation, Angle Dam Volcanics, Spearfelt Rhyodacite.||Felsic volcanics, mafic volcanics including stacked basalt flow units, quartz-feldspar-phyric felsic rocks.|
81055|Gawler Range Volcanics, lower|72462|5|Briefly described|p3, p7-9|Mesoproterozoic|Mesoproterozoic|Gawler Craton. [Also written as Lower Gawler Range Volcanics].|||||Includes felsic and mafic lavas, ignimbrites and tuffs.|
81055|Gawler Range Volcanics, lower|72949|6|Mentioned|p35-37, p39|Calymmian|Calymmian|[Informal subdivision]. Gawler Craton, Olympic Domain, Mount Woods Inlier. Older lower Gawler Range Volcanics locally recognised in Olympic Dam[?] area.|1591-1589 Ma|Gawler Range Volcanics|||A-type mafic to felsic lavas.|
81055|Gawler Range Volcanics, lower|73027|5|Briefly described|p4, p6, p9|Mesoproterozoic|Mesoproterozoic|Central/western Eyre Peninsula.|c. 1592 Ma|||||
81055|Gawler Range Volcanics, lower|73162|6|Mentioned|p447-448, p450, p452-453, p459|Mesoproterozoic|Mesoproterozoic|Gawler Craton. Comprises discrete volcanic centres exposed along margins of the volcanic province.||Gawler Range Volcanics|Angle Dam Dacite, Fresh Well Formation, Roopena Basalt||Rhyolitic to dacitic lavas and pyroclastic successions, less significant mafic lavas.|
81056|Gawler Range Volcanics, upper|67909|4|Described|p124-126, 131, 135-138, 140-141|Mesoproterozoic|Mesoproterozoic||1592-1591 Ma.|Gawler Range Volcanics.|Eucarro Rhyolite.||At least three extensive, porphyritic and compositionally homogeneous felsic (dacite and rhyolite) massive lavas: up to >1000 km3 in volume, up to 300m thick, and 200km across.|
81056|Gawler Range Volcanics, upper|70334|5|Briefly described|p12,75|Calymmian|Calymmian|Geological province: Gawler Craton. Dominantly felsic volcanics. Comprise flat-lying sheets of porphyritic rhyodacite and dacite (Blissett et al., 1993), and represent the most widespread part of the GRV across the central Gawler Craton.||||||
81056|Gawler Range Volcanics, upper|70816|5|Briefly described|p4-5,17|||Gawler Ranges area. Comprises three regionally extensive HT (900-1100 C) felsic lava flows|||Includes Eucarro Rhyolite, Yardea Dacite.|||
81056|Gawler Range Volcanics, upper|70948|6|Mentioned|p975|||Geological province: Gawler Craton. Comprises three regionally extensive, thick (200-300m), high-temperature (900-1100 C) felsic lava flows.||||||
81056|Gawler Range Volcanics, upper|72089|4|Described|p2, p12|Mesoproterozoic|Mesoproterozoic|Gawler Craton. |||Includes the Eucarro Rhyolite and the Yardea Dacite.|||
81056|Gawler Range Volcanics, upper|72462|5|Briefly described|p3, p7-9|Mesoproterozoic|Mesoproterozoic|Gawler Craton. Consists of three regionally extensive thick, felsic lava flows [see Gawler Range Volcanics]. These lava flows are between 200-300 m thick and extend laterally for 80-180 km. Originally interpreted to be ignimbrite deposits. Flows represent high temperature (950-1100oC) lavas. Feature prominent columnar jointing. [Also written as Upper Gawler Range Volcanics].||||||
81056|Gawler Range Volcanics, upper|72949|6|Mentioned|p35-36, p39|Calymmian|Calymmian|[Informal subdivision]. Gawler Craton, Olympic Domain, Mount Woods Inlier. The discrete extrusion age, voluminous nature, and chemical and isotopic homogeneity of the upper Gawler Range Volcanics implies derivation from a mature, well-mixed magma chamber that was efficiently tapped at c. 1.587 Ga.|c. 1587 Ma|Gawler Range Volcanics||Temporally equivalent to felsic lavas of the Benagerie Volcanic Suite.|Includes A-type lavas and ignimbrites. F and volatile-rich.|
81056|Gawler Range Volcanics, upper|73027|6|Mentioned|p4, p6|Mesoproterozoic|Mesoproterozoic|Central/western Eyre Peninsula.|c. 1592 Ma|||||
81056|Gawler Range Volcanics, upper|73162|6|Mentioned|p448, p459|Mesoproterozoic|Mesoproterozoic|Gawler Craton. Volumetrically dominates the Gawler Silicic Large Igneous Province.||Gawler Range Volcanics|||Three regionally extensive, 200-300 m thick felsic lavas.|
24283|Gaylad Sandstone|22560|5|Briefly described|p2|||Gaylad Sandstone overlies a regional unconformity above Pioneer Sandstone and Olympic Formation||||||
24283|Gaylad Sandstone|22561|6|Mentioned|p17|||In the Ooraminna Sub-basin.||||||19-SEP-06
24283|Gaylad Sandstone|22566|4|Described|p81|Neoproterozoic|Neoproterozoic|Stratigraphic relations described - p81.||||||19-SEP-06
24283|Gaylad Sandstone|22648|4|Described|p 132 - 135|||Informally divided into upper and lower Gaylad Sandstone p 132.||||||19-SEP-06
24283|Gaylad Sandstone|22649|2|Defined|p 138-143|Neoproterozoic|Neoproterozoic|The Gaylad Sandstone is tentatively placed midway between 700 and 600 Ma.||||||
24283|Gaylad Sandstone|22762|6|Mentioned|p362|Neoproterozoic|Neoproterozoic|||||||
24283|Gaylad Sandstone|22804|6|Mentioned|p440|||||||||
24283|Gaylad Sandstone|23250|5|Briefly described|p1124 Fig.2||Neoproterozoic III|Correlate of Nucaleena Formation and Tent Hill Formation and Brachina Formation.||||||
24283|Gaylad Sandstone|23287|6|Mentioned|Fig.4|||Age: Lower Ediacarian. Geological province:  Amadeus Basin.||||||19-SEP-06
24283|Gaylad Sandstone|42886|5|Briefly described|Fig.2 P219|||||||||
24283|Gaylad Sandstone|42940|5|Briefly described|Plate 2|Neoproterozoic|Neoproterozoic|Sandstone, conglomerate.  Geological province: Amadeus Basin.||||||23-JAN-08
24283|Gaylad Sandstone|49796|4|Described|p1 & sections|||||||||
24283|Gaylad Sandstone|60549|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Sandstone, feldspathic sandstone, minor granule conglomerate.||||||
24283|Gaylad Sandstone|61732|5|Briefly described|p91, p95|||Lies near the base of the Pertatataka Formation. Geological Province: Amadeus Basin.||||||07-FEB-11
24283|Gaylad Sandstone|62085|6|Mentioned|p24|Ediacaran|Ediacaran|Eastern Amadeus Basin.||||Intertongues with Olympic Formation.||
24283|Gaylad Sandstone|64625|5|Briefly described|p245 fig 2, p252, p254|||Freeman et al. (1991). Amadeus Basin. Previously mapped as Pioneer Sandstone and correlated with the Olympic Formation (Shaw et al., 1983).||||Unconformably overlies Olympic Formation, Pioneer Sandstone, Bitter Springs Formation. Is overlain by Pertatataka Formation.|Clean, medium- to coarse-grained feldspathic sandstone.|
24283|Gaylad Sandstone|64809|6|Mentioned|p10 |||||||||
24283|Gaylad Sandstone|66767|5|Briefly described|p60|Neoproterozoic|Neoproterozoic|NE Amadeus Basin. About 140m thick.||||Unconformably overlies Olympic Formation.|Quartz sandstone, lithic sandstone, subarkose, orthoconglomerate and rare debris-flow diamictite.|
24283|Gaylad Sandstone|69437|5|Briefly described|p22:4-5, 7|Ediacaran|Ediacaran|NE Amadeus Basin, Centralian A Superbasin. Supersequence 3.||||Overlies Olympic Formation. Is overlain by Pertatataka Formation.|Sandstone and conglomerate.|12-JUL-16
24283|Gaylad Sandstone|69438|3|Fully described|p23:2-5, 19|Ediacaran|Ediacaran|Freeman et al. (1991). NE Amadeus Basin. The type section is 17km WNW of Ringwood homestead, on the S flank of the Gaylad Syncline, where it is c.140m thick. Contains four unconformity-bound sequences. Had previously been correlated with Pioneer Sandstone and Olympic Formation. Age estimate is based on dating of units correlated with the underlying Olympic Formation (651 +/- 87 Ma Rb-Sr age for Chambers Bluff Tillite). It could be considerably younger (post-580 Ma) depending on the age of the Elatina Glaciation.|~650 Ma.|||Unconformably overlies Pioneer Sandstone and Olympic Formation. Is overlain conformably by Pertatataka Formation.|Quartz sandstone, lithic sandstone, subarkose, orthoconglomerate (clasts are composed of underlying units) and rare debris-flow diamictite.|12-JUL-16
24283|Gaylad Sandstone|69443|6|Mentioned|p28:10|||Amadeus Basin. Correlates with part of the Mopunga Group (Georgina Basin).||||||12-JUL-16
24283|Gaylad Sandstone|69673|5|Briefly described|p63, p64 fig 53, p88, p91|||||||Conformably overlain by Pertatataka Formation, overlies Pioneer Sandstone|Sandstone and conglomerate.|
24283|Gaylad Sandstone|69937|4|Described|v Fig.1, vi, p3 Tb.1, p22-25, p49-50|Neoproterozoic|Neoproterozoic|NE Amadeus Basin. Type section defined by Field (1991). Possible equivalent to Pioneer Sandstone and Olympic Formation; inferred age range of 700-600 Ma. Zircon age spectrum is in sharp contrast with units above and below. Likely zircon provenance discussed.|1049 +/- 27 Ma (maximum depositional age).|||Unconformably overlies Olympic Formation, Pioneer Sandstone. Is overlain conformably by Pertatataka Formation.|Quartz sandstone, lithic sandstone, subarkose, orthoconglomerate and rare debris-flow diamictite.|
24283|Gaylad Sandstone|70839|5|Briefly described|p329|Ediacaran|Ediacaran|Of Amadeus Basin.||Unit of Pertatataka Formation.||Basal unit of Pertatataka Formation. Underlain by Pioneer Sandstone.||
24283|Gaylad Sandstone|71001|6|Mentioned|p18 Fig.2, p21|Ediacaran|Ediacaran|Amadeus Basin. Fluvial deposits.||||Overlies Olympic Formation. Is overlain by Pertatataka Formation.||
24283|Gaylad Sandstone|71088|6|Mentioned|p8|Neoproterozoic|Neoproterozoic|Amadeus Basin.||||||
24283|Gaylad Sandstone|71279|6|Mentioned|p355 Fig.2|Ediacaran|Ediacaran|Amadeus Basin.||||||
24283|Gaylad Sandstone|71344|5|Briefly described|p1093-1094|||Limited to the north-eastern Amadeus Basin.||Of Pertaoorta Package.||Incised into [unconformable on] Olympic Formation diamictites. Is overlain conformably by Pertatataka Formation.|Yellow to orange, coarse grained, cross-bedded, fluvial sandstone with silty sandstone interbeds.|10-NOV-17
24283|Gaylad Sandstone|71592|5|Briefly described|Appendix A.|||Amadeus Basin.|1049+/-27 Ma (MDA: U-Pb zircon SHRIMP)||||Sandstone.|
24283|Gaylad Sandstone|71841|5|Briefly described|p1|Ediacaran|Ediacaran|Of Amadeus Basin.||||Overlain by Pertatataka Formation.||
24283|Gaylad Sandstone|71842|6|Mentioned|p3|Ediacaran|Ediacaran|Of Amadeus Basin.||||||
24283|Gaylad Sandstone|72369|6|Mentioned|p11-p12|||Of Amadeus Basin. Associated with c. 640-580 Ma Elatina Glaciation (Walter et al., 1995).||||||18-DEC-19
24283|Gaylad Sandstone|72375|4|Described|p1-2,25-26|Neoproterozoic|Neoproterozoic|Of Amadeus Basin. Nomenclature of Freeman et al., 1991.  The type section was originally defined by Field (1991). Confined to NE Amadeus Basin. Depositional age constrained to c. 700-600 Ma based on regional correlations with underlying Olympic Formation (Freeman et al., 1991). Several alternate stratigraphic interpretations include: a) equivalent to upper part of Olympic Formation-Pioneer Sandstone succession (Kennedy and Christie-Blick 2011), b) may represent a localised, proximal equivalent to Waldo Pedlar Member (Pertatataka Formation; P Haines, per comm 2013). Sample location and description are provided. SHRIMP U-Pb zircon analyses by Kositcin et al., 2015 yielded an interpreted maximum depositional age (youngest zircon grain 238U/206Pb) of 1049+\-27 Ma, significantly older than the c. 700-600 Ma depositional age (Freeman et al., 1991). LA-ICP-MS Hf isotopic signatures for the zircon age populations in NTGS AS13CJE018 (feldspathic quartz sandstone) suggest they crystallised in magmas derived from a range of crustal sources (see p26 for Hf isotopic results and interpretations).|c. 700-600 Ma|||Overlain conformably by Pertatataka Formation. Underlain unconformably by Pioneer Sandstone, Olympic Formation.|Quartz sandstone, lithic sandstone, subarkose, orthoconglomerate and rare debris-flow diamictite.|04-DEC-19
24283|Gaylad Sandstone|73085|6|Mentioned|p1|Ediacaran|Ediacaran|||||Underlain by and partly equivalent to Pioneer Sandstone / Olympic Formation. Unconformably overlain by Pertatataka Formation.||
24283|Gaylad Sandstone|73086|2|Defined|p: 3, 5-6, 99, 101, 117-120, 123, 143|||[Defined herein. No revised definition card]. Previously proposed type section was formalized herein. Post-glacial transgressive sandstone unit. Amadeus Basin. Part of Supersequence III. Characterized by pale yellow to pale brown, or grey feldspathic sandstone. Named for Gaylad Creek. Type section: Gaylad Syncline. Key localities: Halfway Dam; Larrier Bore. Distribution: confined to the Fergusson and Gaylad synclines in the northeast of the basin. Difficult to distinguish from sandstones of both the Pioneer Sandstone and Waldo Pedlar Member of the Pertatataka Formation. Two informal subunits: lower unit consists of coarse-grained feldspathic sandstone, and upper unit of gritty sandstone. Thickness at type section: 139 m. Maximum thickness: 182 m, or possibly 240 m (highly variable bedding thickness). No known fossils. Detrital zircon maximum depositional age of 1049 +/- 27 Ma from the unit is much older than the inferred true depositional age, which is at the end of the Marinoan glaciation, i.e. probably ca 635 Ma. Deposited in fluvial- to marine-influenced environments, possibly including lagoonal or lacustrine and marginal marine deltaic environments. Possibly partly correlative to Olympic Formation, Pioneer Sandstone, Pertatataka Formation, Elyuah Formation, Gnallan-a-gea Arkose, Bukalara Sandstone, Buckingham Bay Sandstone.||||Unconformably underlain by Olympic Formation, Loves Creek and Gillen formations (Bitter Springs Group). Conformably[?] overlain by Pertatataka Formation. [See comments].|Fine- to coarse-grained (and rarely granular) lithic and feldspathic sandstone, orthoconglomerate, and minor debris flow diamictite.|
24283|Gaylad Sandstone|73088|6|Mentioned|p1|Cryogenian|Cryogenian|Amadeus Basin, northeast.||||Underlain by Olympic Formation. Unconformably overlain by Pertatataka Formation. Partly equivalent to Pioneer Sandstone.||
24283|Gaylad Sandstone|73180|6|Mentioned|p53|||Amadeus Basin. Possible correlative of the Pioneer Sandstone.||||||
82227|George Hill Iron Member|73230|2|Defined|p6, p9-10, p12, p14-16|Siderian|Siderian|New name [see appendix and ASUD for definition]. Gawler Craton. Domain: Christie and Wilgena. Prospective for iron ore; has several named deposits near Mount Christie. Comprises prominent outcrops of iron-rich gneiss, which contain 30-60 percent typically large grains (100-500 um) of magnetite-martite. Characteristic aeromagnetic signature which indicates strike lengths of 40 km and complex fold structures. Named after George Hill on the TARCOOLA mapsheet. Previously informally known as 'Christie Gneiss unit 2' (Rankin et al., 1996). Type locality: Mount Christie (Rankin et al., 1996). Reference drillhole: GWL023 (266872), interval 24-138 m (total depth). Typically 10-50 m thick, although significantly thicker zones are present in areas of structural thickening by isoclinal folding. Commonly associated with Christie Gneiss and Skuse Hill Metapyroxenite). Maximum deposition age (c. 2480 Ma) and metamorphic age (c. 2460-2415 Ma) derived from adjacent quartz-feldspar-biotite gneiss. May be related to iron-rich lithologies in the Kenella Gneiss but neither unit is well constrained.|c. 2480 Ma (maximum deposition)|Christie Gneiss, Mulgathing Complex|||Iron-rich, quartz magnetite gneiss; predominantly medium- to coarse-grained, quartz-magnetite-diopside-hypersthene-amphibole gneiss, with magnetite, partly altered to martite, and trace sulfides.|
29840|George Mine Formation|22884|2|Defined|p40 Fig. 1, p41||Statherian|Of theThackaringa Group.  Overlies Morialpa Migmatite. Age: 1699+/-10 Ma. Correlates in a general way with Cues Formatuion and Lady Brassey Formation.||||||26-MAR-09
29840|George Mine Formation|62592|6|Mentioned|p14. |||Olary Domain, Curnamona Province.||||||
29840|George Mine Formation|62993|4|Described|p2-p4, p8, 10,12,18, 20, 37-40, 43|Paleoproterozoic|Paleoproterozoic|Age is derived from zircons which show volcanism to be contemporaneous with sedimentation.|1710 Ma, 1718Ma|Wiperaminga Subgroup||Unconformably overlain by Cathedral Rock Formation, overlain by Tommie Wattie Formation|Metagranite, composite gneiss, albititic metasediments, albite granofels, quartzofeldspathic rocks.|19-DEC-21
29840|George Mine Formation|63102|4|Described|p14-19|||Geological province: Olary Domain, Curnamona Province. Nomenclature of Laing (1996b). Albitised metasediment-dominated assemblage (Laing 1996b). Distinguishable from Tommie Wattie and Mooleugore formations by high component of quartz-albitite layers, of felsic volcanogenic derivation from Basso Suite. Upper part of the formation marked by horizon of variable thickness of psammopelitic schist and composite gneiss. Potentially considered to be the albitised equivalent to Tommie Wattie Formation.||Unit of Curnamona Group.||Equivalent to Thackaringa Group, Thorndale Composite Gneiss, Clevedale Migmatite. Overlain by the Ethiudna Subgroup.|Layers of leucocratic, foliated or massive to thickly layered albite - quartz (+\-K-feldspar, biotite, muscovite, magnetite, pyrite) granofels, which is generally interlayered with migmatitic schist (composite gneiss).|22-OCT-19
29840|George Mine Formation|64741|5|Briefly described|p301 Fig. 4, p302|Paleoproterozoic|Paleoproterozoic|Of Wiperaminga Subgp. Overlain by Tommie Wattie Fm.Geol.prov: Olary Domain.Characterised by albitic units of varying thickness, some probably being altered psammites; intervening psammopelitic metasediments have probably been converted to migmatic gneiss||||||07-FEB-11
29840|George Mine Formation|64944|4|Described|p27, p28 Fig. 1, p29 Tb. 1|Paleoproterozoic|Paleoproterozoic|Of Wiperaminga Subgroup (Curnamona Group). Age: ~1718Ma. Pelite, psammite\pelite and psammite, but characterised by albite granofels. Contains numerous magnetite-rich units; volcanic interbeds.||||||07-FEB-11
29840|George Mine Formation|66302|5|Briefly described|p36 Fig.9, p37, p39|Statherian|Statherian|Olary Domain, Curnamona Province. |ca. 1718 Ma|Wiperaminga Subgroup||Overlain by the Mooleugore Formation and the Tommie Wattie Formation.||
29840|George Mine Formation|68126|6|Mentioned|p29|Paleoproterozoic|Paleoproterozoic|Olary Domain, Curnamona Province.||||||
29840|George Mine Formation|70339|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|||Willyama Supergroup.|||Composite gneiss and albitite, interlayered; minor iron formation, exhalite, sulphidic metasediment; quartzite, psammopelite.|27-JAN-16
29840|George Mine Formation|70405|4|Described|p9 table 1, p15, P16,p17 plate 1,p25, |Paleoproterozoic|Paleoproterozoic|Thin mica rich interbeds display strong layer parallel schistosity.Minor banded iron formations.Metasediments commonly flaggy to platy. Migmatites previously named Morialpa Migmatite- term now discontinued. Lacustrine and evaporitic depositional environment.|1710 Ma-1720 Ma|Wiperaminga Subgroup||Underlies Cathedral Rock Formation|Medium grained, quartzofeldspathic metasediment and paragneisses of albitic composition; migmatisation strong throughout. Granofels texture common. Pelitic and psammopelitic schists; pure-feldspathic quartzites & fine-medium grained psammites.|
29840|George Mine Formation|70657|4|Described|p10 Fig.4, p14-15, p17-23, p25-26, p29|Statherian|Statherian|See also p40-41, p44, p59. Laing (1996). Curnamona Province; Olary Domain. Restricted to the Bulloo Subdomain. No equivalent in Broken Hill Domain. Lateral relationship with Mooleugore Formation unknown. Several stratigraphic reference localities are given (Conor, in prep.).|~1718 Ma|Wiperaminga Subgroup||Equivalent to Tommie Wattie Formation. Underlies ?Tommie Wattie Formation and Cathedral Rock Formation (Ethiudna Subgroup), and Oonartra Creek Formation (locally).|Thick upwards fining succession, from psammite to andalusite pelite. Distinguished by high component of quartz-albitite granofels layers. Sedimentary structures are locally spectacularly preserved.|
29840|George Mine Formation|70658|5|Briefly described|p3, 5-10, 15-16, 18-19, 22, 25, 29, 42|Paleoproterozoic|Paleoproterozoic|Olary Domain, Curnamona Province. Oldest known unit of the Willyama Supergroup. Formed eroding horst blocks during deposition of Tommie Wattie Formation in adjoining half-grabens.|c.1718-1715 Ma.|Wiperaminga Subgroup.||Is overlain by Tommie Wattie Formation and, unconformably, by Cathedral Rock Formation.|Metasediments. Typified by albite granofels layers usually interspersed in composite psammopelitic gneiss.|
23612|Germein Bay Formation|40149|6|Mentioned|p122|||||||||
23612|Germein Bay Formation|40976|5|Briefly described|p280|||||||||
23612|Germein Bay Formation|41078|6|Mentioned|p47|||||||||
23612|Germein Bay Formation|41292|6|Mentioned|Fig.1|||||||||
23612|Germein Bay Formation|62577|6|Mentioned|p566|Holocene|Holocene|||||||
80745|Giants Head Suite|72242|4|Described|p29-31,34|Stenian|Stenian|Geological province: Coompana Province, Western Gawler Craton. Comprises both intrusive and extrusive phases. Mantle melt that shows evolved (strongly negative) EHF1074 Ma values. Indicating contamination by a <1900 Ma crustal substrate. Temporal equivalent to Giles Suite, Musgrave Province, and therefore raises the Ni-CU PGE potential.|c. 1077 Ma|Unit of Warakurna Supersuite.|||Amygloidal olivine basalt lava flows; olivine dolerite-gabbro plutons, quenched basaltic dykes.|
80745|Giants Head Suite|72344|5|Briefly described|p3, p7, p9, p35, p44|Stenian|Stenian|Coompana Province. Petrography, SHRIMP analyses and geochemistry are discussed for several samples.|1074 +/- 6 Ma (Magmatic SHRIMP age)|Warakurna Supersuite|Includes the Warbla Basalt and the Mallabie Basalt.|||
80745|Giants Head Suite|72947|2|Defined|p7-9, p11-12, p16-p21|Stenian|Stenian|Coompana Province, southeastern. Named after Giants Head Cave. Type locality: CDP002 (drillhole 299056, interval 374.47-445.85 m). Product of mantle melting derived from heterogeneous lithospheric mantle. Evolved (strongly negative) eHf1074 Ma values indicating contamination by a >1900 Ma crust. Similar timing and the same remnant magnetic signature as Warbla Suite but geochemically distinct; suggests they are not genetically related and had different sources. Four types of intrusions based on aeromagnetic images. Sharp, transgressive contacts with host units. Geochemical composition suggest it was derived from a source that included unradiogenic older crustal material not sampled by the Warbla Suite.|1074 +/- 6 Ma SHRIMP U-Pb|Warakurna Supersuite|Includes Mallabie Basalt.|Intrudes the Koomalboogurra, Bunburra and Koonalda suites.|Olivine-bearing mafic intrusive rocks. Dominantly dark green to pale grey, fine- to coarse-grained dolerite that ranges from inequigranular to porphyritic. Also occurs as dark grey, massive, aphyric basalts that form dykes that intrude other units.|
80745|Giants Head Suite|73091|5|Briefly described|map legend|Stenian|Stenian||c. 1077 Ma|Warakurna Supersuite|||Amygdaloidal olivine basalt flows and olivine dolerite-gabbro plutons with quenched dykes.|30-NOV-21
80745|Giants Head Suite|73224|5|Briefly described|p42|Stenian|Stenian|Produced from intraplate magmatism; result from melting heterogeneous lithospheric mantle. Magma was contaminated by 1900 Ma crust, as indicated by strongly negative eHf values.|c. 1074 Ma|Warakurna Supersuite||||
80745|Giants Head Suite|73225|5|Briefly described|p4||||c.1074 Ma.|Warakurna Supersuite.||Correlated with Giles Complex.|Intrusive and extrusive mafic magmatism.|
80745|Giants Head Suite|73641|5|Briefly described|p2, 4||||~1075 Ma|Warakurna Supersuite|Mallabie Basalt|Likely the intrusive feeder system to Mallabie Basalt. Intrudes Koomalboogurra, Bunburra, Koonalda Suites and Moodini Supersuite.||
78311|Gibbon beds|68715|6|Mentioned|p31 Fig.5, p32 Fig.6|Pliocene|Pliocene|Western Pirie Basin.||||||
78311|Gibbon beds|70334|5|Briefly described|p60|Pleistocene|Pliocene|"Of Pirie Basin. Thickness: 4-25m on CULTANA. Deposited in a lacustrine-deltaic environment and are probably Pliocene-Pleistocene in age (Parker and Fanning, 1998). Intersected in numerous drillholes 24200, 24205, 24211, 24213, 24234, 24251, 161174, 166738, 179299,||||Underlain by Melton Limestone.|Red, yellow and grey mottled clay-rich sand and clay.|
78311|Gibbon beds|73103|5|Briefly described|Map legend.|Pleistocene|Pliocene||||||Mottled clayey sand, sandy clay, conglomerate. Non-marine.|
24285|Giddinna Formation|38604|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
24285|Giddinna Formation|38605|4|Described|p40|||||||||
24285|Giddinna Formation|42469|6|Mentioned|p48|||||||||
24285|Giddinna Formation|42723|6|Mentioned|map legend|Pleistocene||||||||
24285|Giddinna Formation|43048|6|Mentioned|p24|||||||||
24285|Giddinna Formation|43053|5|Briefly described|Map Legend|Pleistocene|Pleistocene|||||||25-MAY-05
24285|Giddinna Formation|43258|5|Briefly described|Map Legend|Holocene|Pleistocene|||||||
24285|Giddinna Formation|43298|6|Mentioned|Map Legend|Holocene|Pleistocene|||||||
24285|Giddinna Formation|44133|5|Briefly described|p243|Quaternary|Quaternary|Underlain by Bulldog Shale. Pleistocene Palaeosol occurs within this unit.||||||
24285|Giddinna Formation|60953|5|Briefly described|Map Legend|Pleistocene|Pleistocene|Gravelly and sandy clay, commonly gypcreted or calcreted.||||||
24285|Giddinna Formation|61108|5|Briefly described|map legend|Pleistocene|Pleistocene|Gravelly and sandy clay of piedmont slopes and alluvial plains, commonly gypcreted or calcreted.||||||31-MAY-05
25922|Gilberts Sand|38290|2|Defined|p46|Quaternary|Quaternary|||||||
80748|Gilgerabbie Suite|72242|5|Briefly described|p29-31|Calymmian|Calymmian|Geological province: Coompana Province. Post-dates Kararan Orogeny. Nomenclature of Wade et al. (2007). Interpreted to be magmatic product of intracontinental extension after cessation of c. 1526 Ma subduction event (Smithies et al., 2015).|c. 1500 Ma||||Granitic gneiss.|
80748|Gilgerabbie Suite|72344|6|Mentioned|p3, p7|Calymmian|Calymmian|Coompana Province. Intersected in drillhole Mallabie 1.|c. 1500 Ma|Undawidgi Supersuite|||Migmatitic orthogneiss.|
80748|Gilgerabbie Suite|72934|6|Mentioned|p2|||Geochemically and temporally similar to the Undawidgi Supersuite.||||||
80748|Gilgerabbie Suite|72947|2|Defined|p7-9, p13-14, p21|Calymmian|Calymmian|Coompana Province, eastern. Named after Gilgerabbie Bore. No known surface exposures. Type locality: Mallabie 1 (drillhole 353, composite section including two intervals 1404.20-1406.00 m and 1493.50-1495.63 m). Unconformably overlain by 135.3 m of coarse-grained arkosic sandstone with a maximum depositional age of 1151 Ma. Interpreted to be the product of intracontinental extension (Smithies et al., 2015) following cessation of c. 1526 Ma subduction. In thin section, the rock has leucocratic zones of granoblastic textured quartz, plagioclase and microcline that alternate with parallel irregular lenses of biotite, hornblende, garnet, titanate and opaque minerals.|1505 +/- 7 Ma and 1500 +/- 8 Ma SHRIMP U-Pb|Undawidgi Supersuite||Appears to intrude the Koomalboogurra Suite.|Coarse-grained, moderately foliated granitic gneiss.|
80748|Gilgerabbie Suite|73091|5|Briefly described|map legend|Calymmian|Calymmian||c. 1500 Ma|Undawidgi Supersuite|||Granitic gneiss.|30-NOV-21
80748|Gilgerabbie Suite|73224|6|Mentioned|p42|Calymmian|Calymmian|Coompana Province, eastern.|c. 1505 Ma|Undawidgi Supersuite||||
80748|Gilgerabbie Suite|73225|6|Mentioned|p4|||||Undawidgie Supersuite.||||
80748|Gilgerabbie Suite|73641|6|Mentioned|p4|||||Undawidgi Supersuite||||
68739|Gleesons Landing Granite|24585|5|Briefly described|p32||Paleoproterozoic|Of the Donington Suite. I-type granite. Felsic and mafic plutons intrude the Corny Point Paragneiss. Age: ~1855Ma (for early phases). Intruded by the Royston Granite.||||||23-DEC-09
68739|Gleesons Landing Granite|60958|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Massive to banded I-type granitoid pluton or sill complex. Of the Donington Suite. Geological Province: Gawler Craton.||||||07-NOV-08
68739|Gleesons Landing Granite|61121|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Massive to banded I-type granitoid pluton or sill complex. Intruded by Jussieu Metadolerite. Geological Province: Gawler Craton.||||||07-NOV-08
68739|Gleesons Landing Granite|64282|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Geol Prov: Gawler Craton. Massive to banded I-type granitoid pluton or sill complex. Includes syenogranite (1855-1850Ma), adamellite, granodiorite (Rb-Sr age: 1808+/-18Ma), augen orthogneiss (1850+/-5Ma), hornblende micro-adamellite and biotite schist.||||||07-NOV-08
68739|Gleesons Landing Granite|64313|5|Briefly described|p452-456|Paleoproterozoic|Paleoproterozoic|Of the Donington Suite. Age: 1850+/-5, 1850+/-3 and 1850+/-2Ma. Includes syenogranite, adamellite, granodiorite and augen orthogneiss, all foliated and migmatised.  Intruded by Royston Granite. Whole rock chemistry included.||||||09-FEB-10
68739|Gleesons Landing Granite|65219|6|Mentioned|p28 Fig.2|Paleoproterzoic|Paleoproterzoic|Unit within Donington Suite||||||22-SEP-09
68739|Gleesons Landing Granite|65375|4|Described|p7, pp12-20, p44.|Paleoproterozoic|Paleoproterozoic|Southern part of Yorke Peninsula. Type locality is at Gleesons Landing. A group of massive to banded granitoid plutons or sill complexes; usually standing out against coastal erosion. I-type granite. Early phases intruded by megacrystic augen orthogneiss c.1850 Ma. Shows four distinct deformation structures and fabrics. The syenogranite phase is equivalent to Colbert Granite on Eyre Peninsula; the augen orthogneiss phase correlates with the Wanna Megacrystic Granite Gneiss on Eyre Peninsula.|c.1855-1850 Ma.|Unit in Donington Suite.||Intrudes Corny Point Paragneiss. Intruded by Royston Granite and Tournefort Metadolerite.|Four phases identified: syenogranite, adamellite, granodiorite, augen orthogneiss; locally partly intercalated; generally foliated, layered and folded.|
68739|Gleesons Landing Granite|66302|6|Mentioned|p27|Orosirian|Orosirian|Ages from Jagodzinski et al. (2006). |1850 +/- 5 Ma to 1850 +/- 3 Ma (SHRIMP U-Pb)|Donington Suite||||
68739|Gleesons Landing Granite|68131|5|Briefly described|p3 Tb.1, p7-16, p23-p24|||Dated sample is a megacrystic granite gneiss. Is equivalent to Augen Orthogneiss described by Zang (2002) and to the Wanna Megacrystic Granite Gneiss of Schwarz (2003). Deformed by structures formed prior to the emplacement of the Royston Granite.|1850 +/- 2 Ma.|Donington Suite.||Is intruded by Royston Granite.|Layered granite gneiss, discordantly migmatised granodiorite gneiss, megacrystic granite gneiss.|18-JAN-22
68739|Gleesons Landing Granite|73092|6|Mentioned|p3, p15|Orosirian|Orosirian|Age is of magmatic crystallisation. Dated sample is augen gneiss from Berry Bay. This age is within uncertainty of other zircon crystallisation ages for the Donington Suite.|1834 +/- 18 Ma|Donington Suite|||Includes megacrystic granite with coarse K-feldspar and a foliation defined by biotite, hornblende and quartz-feldspar.|
68739|Gleesons Landing Granite|73107|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Gawler Craton: Yorke Peninsula, islands of Investigator Strait and DDH Investigator 1. Massive to banded granitoid pluton or sill complex. Four facies are mapped separately. The syenogranite is dated at ~1855-1850 Ma; granodiorite at 1808 +/- 18 Ma (Rb-Sr); augen orthogneiss at 1850 +/- 5 Ma.||Donington Suite.||The granodiorite facies intrudes Corny Point Paragneiss. Is intruded by Royston Granite.|Includes syenogranite (fine to medium-grained, foliated and layered); adamellite (foliated, intercalated with syenogranite); granodiorite (transitional to tonalite, foliated); augen orthogneiss (strongly deformed, megacrystic). I-type.|
68739|Gleesons Landing Granite|73525|5|Briefly described|p19 Fig.13|Orosirian|Orosirian|Olympic Domain.|1850+/-5 Ma crystallisation age|Donington Suite|||Felsic intrusive.|
34776|Glen Osmond Slate Member|22889|4|Described|p35 & p39|Adelaidean|Adelaidean|For location of type section see p39. Superseds the former Glen Osmond Slate as the unit has been down graded from formation to member status, see p35 for details of the change.||||||
31513|Glenforslan Formation|23179|5|Briefly described|p32, Fig.2||Middle Miocene|Fossil assemblage includes whale bones.||||||
31513|Glenforslan Formation|23226|2|Defined|p898||Batesfordian|Was previously the informal unit - Lower Morgan Limestone. Identification of diverse bryozoan assemblages very important as over/underlying units have very similar lithology. Of Morgan Group.||||||
31513|Glenforslan Formation|23768|5|Briefly described|p34|||Recognised by Lukasik and James (1993) as a distinct unit of Morgan Limestone which is now recognised as a group. Geological Province: Murray Basin.||||||10-MAR-05
31513|Glenforslan Formation|24558|4|Described|p655 Fig. 3|Middle Miocene|Middle Miocene|Low energy carbonate ramp sediments with with abundant bryozoans and molluscs. Conformably overlies Finnis Formation; conformably overlain by Cadell Formation.||||||
31513|Glenforslan Formation|60785|5|Briefly described|p184 Fig.1, p196.  |Langhian|Burdigalian|South Australia. Presence of Lepidocyclina howchini indicates Batesfordian age (early Middle Miocene) (Lukasik and James, 1998). Has yielded fossil cetacean elements including one almost complete cranium.|||||Bryozoal calcarenite.|
31513|Glenforslan Formation|63460|4|Described|p847-848|Early Miocene|Early Miocene|Of the Morgan Group. Overlies Finniss Formation; underlies Cadell Fm. Thickness: 40m. Geological province: Murray Basin. Calcarenite and calcisiltite interbedded with marl in outcrop; base is foraminiferal limestone. Misspelt in all the diagrams as Glensforlan Formation.Shown [correctly] as Glenforslan Formationin text. p847.||||||08-SEP-20
31513|Glenforslan Formation|64237|5|Briefly described|p19 Fig. 2b|Early Miocene|Early Miocene|Introduced as a constituent of the Morgan Group (Murray Supergroup) by Lukasik and James (1998) - and became a constituent of the nMorgan Subgroup when the Murray Group was reinstated. Occurs between the Cadell Formation above and Finniss Formation below.||||||29-JUL-08
31513|Glenforslan Formation|68716|6|Mentioned|p39 Fig.3|||||||Overlain by the Winnambool Formation.||
79740|Gluepot Granite|71037|5|Briefly described|p22-23 Fig.2, p27 Fig.6|Paleoproterozoic|Paleoproterozoic|Dating 207Pb/206Pb TIMS age c. 1740 Ma.|c. 1740 Ma.|Of Moola Suite.||Shown as younger than Wandearah Formation.|Porphyritic granite composed of large pink K-feldspar phenocrysts in a plagioclase-K-feldspar-quartz-biotite-tourmaline matrix. Contains medium-grained granite, late stage, microgranite, pegmatite, aplite, quartz porphyry dykes and plugs.|
79740|Gluepot Granite|71129|4|Described|p31,35,40,42-45,74,105,177|Statherian|Statherian|Geological Province: Olympic Domain, Gawler Craton. Dimensions: ~25 x 6 km large N-NW-trending pluton extending from Angle Dam to Wild Dog Hill, northeast of Whyalla. An elliptical magnetic high in regional TMI imagery. Poorly exposed, dominated by subcrop, deeply weathered. Intruded into Moonabie Formatio nduring kimban Orogeny; intrusive contact with Moonabie Formation represented by breccia zones of tabular to rounded quartzite clasts in a tourmaline matrix. Compositionally ranges from magnesian, alkali-calcic to calc-alkalic magnesian. HREE-enriched, with moderate to distinctly negative Eu anomalies, interpreted to be derived from crustal melting. Previously interpreted to be part of Hiltaba Suite, but recognised to be of Moola Suite based on recent geochronology analysis. Geochronological ages are within error of the Wortham Granite; SHRIMP U-Pb magmatic age of 1752+\-10 Ma of a quartz-phyric rhyolite plug, and U-Pb CA-TIMS age of c. 1740 Ma for a foliated equigranular facies of Gluepot Granite (J. Crowley, pers. comm. 2016). Lithology is discussed in some detail. See also p179-182,184,199,201,225,227, app 239, app 241.|c. 1740 Ma (magmatic; Pb/Pb TIMS)|Unit of Moola Suite.||Intrudes into Moonabie Formation.|Coarse-grained porphyritic to medium-grained equigranular K-feldspar quartz-biotite granite in addition to late stage pegmatite and aplite phases.|13-NOV-19
79740|Gluepot Granite|71130|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic||c.1740 Ma (207Pb/206Pb TIMS age).||||Pink K-feldspar-phyric granite in a medium-grained plagioclase-K feldspar-quartz-biotite-tourmaline matrix. Contains phases of equigranular, medium-grained granite, late stage microgranite, pegmatite, aplite, quartz porphyry dykes and plugs.|
79740|Gluepot Granite|71131|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic||c.1740 Ma (207Pb/206Pb TIMS age).|Moola Suite.|||Pink K-feldspar-phyric granite in a medium-grained plagioclase-K feldspar-quartz-biotite-tourmaline matrix. Contains phases of equigranular, medium-grained granite, late stage microgranite, pegmatite, aplite, quartz porphyry dykes and plugs.|
79740|Gluepot Granite|71414|6|Mentioned|p43|Statherian|Statherian|Geological province: Gawler Craton.|~1740 Ma|||Intrudes Moonabie Formation.||
79740|Gluepot Granite|71862|2|Defined|p6-p7 , p9-p10, p25|Statherian|Statherian|Named for the Gluepot Dam and is a north-northwest trending pluton approximately 25km long and 6km wide extending from Angle Dam near Roopena Homestead to Wild Dog Hill near Whyalla in the south on Roopena Station. The type locality is the small hill with prominent granite tors 1.3km north-northwest of Whyalla Dam. It comprises the area extending 100m radially from the point 725210mE, 6367995N, GDA94, Zone 53. A reference locality for the gneissic phase is 1.7km NW of Speck Dam comprising the area extending 100m radially from the point 724686mE, 6365829mN, GDA94, Zone 53. This unit is poorly exposed and dominated by subcrop and saprolitic granite with isolated platform exposures and rare granite hills and tors. A quartz-phyric rhyolite plug is interpreted to be related to the Gluepot Granite and has a magmatic age of 1752 +/- 10 Ma (Fraser and Neumann, 2010). Geochemistry is discussed. See also p28-p29, p53, p56-p57.|c. 1740 +/- 0.6 Ma (CA-TIMS, McAveny et al, 2017)|Moola Suite||Intrudes the Moonabie Formation.|Coarse-grained porphyritic granite, medium-grained equigranular granite and late stage pegmatites and aplites.|18-APR-23
79740|Gluepot Granite|73110|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic||1740 Ma (207Pb/206Pb TIMS).|Moola Suite.|||Granite, mostly porphyritic, large pink K-feldspar phenocrysts, groundmass of m.g.-c.g. plagioclase, K-feldspar, quartz, biotite, minor tourmaline; late stage microgranite, pegmatite, aplite, quartz porphyry dykes and plugs.|
79740|Gluepot Granite|73525|5|Briefly described|p19 Fig.13|Statherian|Statherian|Olympic Domain.|1740+/-1 Ma crystallisation age|Moola Suite|||Felsic intrusive.|
23623|Golden Pole Granite|22631|6|Mentioned|p176|Calymmian|Calymmian|||||||
23623|Golden Pole Granite|24197|5|Briefly described|p75 Tb. 8.1|Mesoproterozoic|Mesoproterozoic|Age: 1560Ma.||||||07-FEB-11
23623|Golden Pole Granite|42885|2|Defined|p23||Mesoproterozoic|see also Fig.3 p24||||||12-NOV-14
23623|Golden Pole Granite|43052|5|Briefly described|Table 5.12|||||||||
23623|Golden Pole Granite|50605|5|Briefly described|P(iii), 1.4, 10.2, Table 1.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Gawler Craton & Curnamona Province. Of the Moolawatana Suite.||||||
23623|Golden Pole Granite|68068|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Curnamona Province.||Unit in Moolawatana Suite.|||Mostly non-porphyritic, reddish, xenolith-free, tourmaline-rich, fine- to coarse-grained biotite granite, composed of K-feldspar, plagioclase, quartz and biotite with accessory tourmaline, opaques, apatite, locally scheelite and copper sulfides.|
23623|Golden Pole Granite|69023|4|Described|p26, p30-31, p35-37, p47-50, p189|Mesoproterozoic|Mesoproterozoic|Of Teale (1993); previously included in Mount Neill Granite Porphyry by Coats et al. (1969). Type area is around the Mount Fitton South Copper Mine. Mount Painter Inlier. Geochemistry detailed. Age inferred from stratigraphic relationships.||Unit in Moolawatana Suite.||Intrudes Terrapinna and Wattleowie Granites. Is overlain unconformably by Fitton Formation.|Usually non-porphyritic, brick-red, xenolith-free and tourmaline-rich; wide range in grain size; tourmaline-quartz clots are relatively common. Local hydrothermal alteration with Cu mineralisation.|
23623|Golden Pole Granite|69562|5|Briefly described|p671 Tb.5||||1560 Ma (Wall, 1995).||||Even-textured, brick-red-coloured granite.|
23623|Golden Pole Granite|70384|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Scheelite and copper sulfides occur locally as accessory minerals.|||||Mostly non-porphyritic, reddish, xenolith-free, tourmaline-rich (orbicules and clots), fine- to coarse-grained biotite granite. Composed of K-feldspar, plagioclase, quartz and biotite; accessory tourmaline, opaques, apatite.|
39203|Goodwood Formation|23768|5|Briefly described|p30 Fig.6, p27|Late Miocene|Late Miocene|Geological Province: Otway Basin. See also p33, p162.||||||30-MAR-05
36996|Hall Bay Volcanics|23491|2|Defined|p19|Archean|Archean|Age: ~2520 Ma+/-7 Ma. Felsic metavolcanic unit. Intruded by Kiana Granite and Coulta Granodiorite.||||||07-NOV-08
36996|Hall Bay Volcanics|24365|6|Mentioned|p4|||||||||
36996|Hall Bay Volcanics|61070|5|Briefly described|Map Legend|Proterozoic|Archean|Of the Sleaford Complex. Compositionally layered felsic metavolcanics and/or epiclastics including magnetite-rich and carbonaceous units and amphibole-rich intrusives. Age: 2520 +/- 7Ma (U-Pb Zircon). Geological Province: Gawler Craton.||||||23-JUL-13
36996|Hall Bay Volcanics|63866|5|Briefly described|p3, p18|Proterozoic|Archaean|Coulta Domain, Gawler Craton. |c. 2525 Ma||||Felsic volcanic and volcaniclastic units.|
36996|Hall Bay Volcanics|64130|6|Mentioned|p1379 |||Prospective for volcanic-associated metal sulfide and magmatic sulfide mineralisation.|c.2520 Ma (Teale et al., 2000).||||Plume-related komatiites and mafic volcanics.|
36996|Hall Bay Volcanics|64313|5|Briefly described|p450 Fig. 1|Archean|Archean|Age: 2521+/-6Ma (U-Pb zircon). Geological province: Gawler Craton.||||||09-FEB-10
36996|Hall Bay Volcanics|64722|6|Mentioned|p12|Neoarchean|Neoarchean|Of (or intrudes?) Sleaford Complex, Gawler Province. Emplaced as part of igneous activity between 2650 and 2500 Ma.||||||
36996|Hall Bay Volcanics|64828|5|Briefly described|p1065, p1067|Archean|Archean|Included in the Sleaford Complex. Overlain by Price Metasediments. Greenschist facies/chloritoid-andalusite-bearing rocks.||||||04-MAR-09
36996|Hall Bay Volcanics|65376|4|Described|p11, p15, pp23-32.|Archean|Archean|Low-grade metamorphism from c.2500-2400 Ma Sleafordian Orogeny. Does not outcrop. Prospective for VHMS mineralisation.|2521 +/- 6 Ma.|||Intruded by Dutton Suite and Kiana Granite.|Metamorphosed felsic and mafic volcanics and iron-rich sediments. Contains corroded and embayed quartz and K-feldspar phenocrysts in a generally finer grained groundmass.|
36996|Hall Bay Volcanics|65485|6|Mentioned|p42|Archean|Archean|Greenschist facies unit of the Sleaford Complex.||||||19-MAR-12
36996|Hall Bay Volcanics|65915|5|Briefly described|p2, p3 Fig.2|Neoarchean|Neoarchean|In southwestern Eyre Peninsula. ~2520 Ma (Fanning et al., 2007).||||||
36996|Hall Bay Volcanics|66302|5|Briefly described|p10-p14, p60, p61, p61 Fig.14, p85|Neoarchean|Neoarchean|Christie and Wilgena Domains, Gawler Craton. Interpreted to have its origin in the same magmatic system as the Glenloth Granite, Devils Playground Volcanics and the Coulta Granodiorite. SHRIMP U-Pb zircon ages from Swain et al. (2005) and Fanning et al. (2007).|2529 +/- 4 Ma to 2517 +/- 7 Ma |Sleaford Complex|||Low metamorphic grade aluminous metapelites interlayered with felsic (dacitic and rhyolitic) volcanic and volcaniclastic units.|
36996|Hall Bay Volcanics|66882|6|Mentioned|p116|Neoarchean|Neoarchean|Contains inherited c.2700 and c.2570 Ma zircons from the Gawler Craton basement.|2520-2500 Ma|||||
36996|Hall Bay Volcanics|67058|5|Briefly described|p476.|Neoarchean|Neoarchean|Southern Gawler Craton.||Unit in Sleaford Complex.||||
36996|Hall Bay Volcanics|67536|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Gawler Craton.|2520 +/- 7 Ma||||Felsic metavolcanic rocks and metasediments.|02-APR-14
36996|Hall Bay Volcanics|67721|5|Briefly described|p36|Neoarchean|Neoarchean||c. 2520 Ma|||||
36996|Hall Bay Volcanics|68128|5|Briefly described|p2, p6-7|||Gawler Craton. Originally defined by Teale, Schwarz and Fanning (2000).|ca. 2520-2530 Ma (U-Pb)|Sleaford Complex|||Altered felsic volcanics and probable epiclastics.|
36996|Hall Bay Volcanics|68208|6|Mentioned|p31 Fig.2, p39|Paleoproterozoic|Neoarchean|Minimum detrital zircon age ~2510 Ma.||Of Sleaford Complex||||
36996|Hall Bay Volcanics|69203|5|Briefly described|p35|||Southern Gawler Craton.|c.2530-2520 Ma.|Sleaford Complex.||||
36996|Hall Bay Volcanics|69554|6|Mentioned|p136|||Fanning et al. (2007). Southern Gawler Craton.|c.2530-2520 Ma.|||||
36996|Hall Bay Volcanics|70027|6|Mentioned|p56|Archean|Archean|Geological province: Gawler Craton.||||||
36996|Hall Bay Volcanics|71043|5|Briefly described|p115|Neoarchean|Neoarchean|Ages by Swain et al. (2005) and Fanning et al. (2007) respectively.|2529 +/- 3.6 Ma; 2517 +/- 7 Ma.|Sleaford Complex.||||
36996|Hall Bay Volcanics|71235|6|Mentioned|p14||||2520-2500 Ma (Fanning et al., 2007)|||||
36996|Hall Bay Volcanics|71859|5|Briefly described|p2, p6-p8, p14, p16, p28, p36|Neoarchean|Neoarchean|Southern Gawler Craton. Known only from drillholes near Mount Hope.|2520 +/- 7 Ma (Teale et al., 2000)|Sleaford Complex||Intruded by the Kiana Granite and Coulta Granodiorite.|Felsic volcanics and volcaniclastics interlayered with aluminous metapelites and evaporitic and iron-rich sediments.|
36996|Hall Bay Volcanics|73026|5|Briefly described|p9|Paleoproterozoic|Archean||c. 2520 Ma||||Felsic metavolcanics; epiclastics; metasandstone.|
36996|Hall Bay Volcanics|73027|5|Briefly described|p9,|Palaeoproterozoic|Archaean||c. 2520 Ma||||Felsic metavolcanics, epiclastics and metasandstone.|
36996|Hall Bay Volcanics|73104|6|Mentioned|p1|Neoarchean|Neoarchean||c. 2520 Ma|||||
36996|Hall Bay Volcanics|73235|6|Mentioned|p56|||Hosts gold mineralisation in the Hall Bay mineral field of the Sleafordian gold mineral system.|||||[May include banded iron formation and gneiss].|
36996|Hall Bay Volcanics|73256|6|Mentioned|p559|||||Sleaford Complex|||Medium- to high-grade metamorphics.|
27794|Hamilton Creek Member|22510|5|Briefly described|table1p37|||Of the Fitton Formation.  Age: Sturtian. Northern Flinders Ranges.||||||13-OCT-04
27794|Hamilton Creek Member|41647|4|Described|p834|||||||||
27794|Hamilton Creek Member|68068|5|Briefly described|Map legend|Sturtian|Sturtian|||Unit in Fitton Formation.|||Granite clasts to 2 m diameter with an arkosic to silty matrix; clasts subangular to well-rounded, partly deformed by later folding; ranges from clast to matrix supported from base upwards; the top is often gradational with rest of Fitton Formation.|
27794|Hamilton Creek Member|69019|4|Described|p42, p44, p144.|Neoproterozoic|Neoproterozoic|Young and Gostin (1989); formally named the 'granite conglomerate member' or 'tillite member' of Coats (1962) and Coats et al. (1969). Weathered regolith in/on crystalline basement; resembles a 'tor and grus' colluvial deposit.||Unit in basal Fitton Formation.|||Rounded to subrounded granite clasts (gravel to boulder size); matrix size decreases upwards from meta-arkosic grit to greywacke sand to siltstone; calc-silicate bands.|
27794|Hamilton Creek Member|69023|5|Briefly described|p61-62, p64-65, p147|Neoproterozoic|Neoproterozoic|Clasts sourced from local crystalline basement and moved by water +/- ice a short distance overland.||Basal unit in Fitton Formation.|||Conglomerate with (sub)rounded granite clasts up to more than 3m in size, a fining-upwards matrix from meta-arkosic grit to greywacke sand to siltstone; locally includes hornfelsed calcareous tillite and a calc-silicate rock with quartz clasts.|
27794|Hamilton Creek Member|70384|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Adelaide Geosyncline.  Age shown more specifically as Sturtian [Cryogenian].||Of Fitton Formation.|||Sandstone-conglomerate, clasts mostly granite (<2m wide, subangular to well rounded, partly tectonically deformed) in arkosic sandstone to silt matrix, grey to olive-grey. Grades upward from dominantly clast to matrix supported; top is gradational.|21-JAN-19
27794|Hamilton Creek Member|72456|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Marree 1:250k map sheet. |||||Grey to olive laminated silty mudstone, granule to boulder sandy conglomerate; sandstone; diamictite, locally with abundant granite clasts.|
38060|Hammerhead Supersequence|23792|5|Briefly described|p47|Late Cretaceous|Late Cretaceous|Equivalent to Potoroo Formation. See also Hammerhead supersequence. Geological Provice: Bight Basin. Off shore.||||||04-MAY-05
38060|Hammerhead Supersequence|24336|5|Briefly described|p99 Fig.3|||Correlated to the Potoroo Formation.||||||
38060|Hammerhead Supersequence|61544|6|Mentioned|p367 Fig.3. |Maastrichtian|Santonian|Ceduna Sub-basin. Post-break-up thermal subsidence.||||Overlies Tiger Supersequence.||
38060|Hammerhead Supersequence|66578|5|Briefly described|pp1005-1007, p1010.|Late Cretaceous|Late Cretaceous|Ceduna Sub-Basin. c.3.5km thick. Sand-rich, believed to have been deposited very quickly from a local source. Host to a Delta-Deepwater Fold-Thrust Belt formed by gravity gliding, driven primarily by sediment supply, not gradient.||||Overlies Tiger Supersequence. Is overlain unconformably by Wobbegong and Dugong Supersequences.||
38060|Hammerhead Supersequence|69297|5|Briefly described|p14 fig 2.4, p23, p25 fig 2.9|Danian|Campanian|Ceduna and Duntroon Sub-basins. Maximum thickness of approximately 5000m. See also p37, p38, p41-p44, p46, p58, p60, p61.  ||||||
38060|Hammerhead Supersequence|70067|5|Briefly described|Ceduna: Fig.2;p1-2. Regional: Fig.2;p2-5|Maastrichtian|Santonian|Bight Basin. Comprises Potoroo Formation. Deltaic and shallow marine sandstones are potential oil and gas reservoirs according to petroleum systems modelling; marine shales are intraformational seals. Also sealed by thick transgressive marls at the base of the Dugong Supersequence.||||Overlies Tiger Supersequence. Is overlain by Wobbegong Supersequence.|Includes deltaic sandstones.|
25940|Hampton Sandstone|14227|5|Briefly described|Enclos. 2|Late Eocene|Middle Eocene|Presented as Princess Royal Spongolite, Hampton SS.||||||07-FEB-11
25940|Hampton Sandstone|22587|6|Mentioned|p79 Fig.7|Late Eocene|Middle Eocene|||||||
25940|Hampton Sandstone|22613|4|Described|p20|Late Eocene|Middle Eocene|||||||
25940|Hampton Sandstone|22614|5|Briefly described|map|Eocene|Eocene|||||||
25940|Hampton Sandstone|22626|6|Mentioned|439 fig 3|Eocene|Eocene|Geol province Eucla Basin. Max thickness 85 m.  Overlying unit Wilson Bluff Limestone.||||||21-OCT-08
25940|Hampton Sandstone|23138|5|Briefly described|p240|||||||||
25940|Hampton Sandstone|23331|5|Briefly described|1089 Fig.2|Middle Eocene|Middle Eocene|||||||
25940|Hampton Sandstone|23488|5|Briefly described|p36, p38 Fig. 3|Eocene|Eocene|Overlies the Paling Member.  Geological Province: Eucla Basin.||||||
25940|Hampton Sandstone|23533|5|Briefly described|p564 Fig 3|Middle Eocene||Geological Province: Bremer Basin.||||||
25940|Hampton Sandstone|23582|5|Briefly described|Map Legend|Eocene|Eocene|Of Eundynie Group. Poorly sorted sandstone, typically quartz rich; includes subordinate gravel, conglomerate and siltstone.||||||27-JUN-06
25940|Hampton Sandstone|23584|5|Briefly described|p29|Late Eocene|Eocene|Of Eundynie Group. Geological Province: Yilgarn Craton.||||||
25940|Hampton Sandstone|23989|5|Briefly described|p56|Late Eocene|Early Eocene|Geological Province: Yilgarn Craton. See also misspelt Hampton Formation in this paper.||||||03-MAR-10
25940|Hampton Sandstone|24057|5|Briefly described|p97|Tertiary|Tertiary|Geological Basin: Eucla Basin.||||||
25940|Hampton Sandstone|24094|6|Mentioned|p271|||Geological Province: Eucla Basin||||||16-MAR-05
25940|Hampton Sandstone|24324|5|Briefly described|p27|Early Eocene|Late Paleocene|Geological Province: Eucla Basin||||||
25940|Hampton Sandstone|24347|5|Briefly described|p121|Middle Eocene|Middle Eocene|Overlying unit: Wilson Bluff Limestone. Maximum thickness 30m.||||||27-JUL-09
25940|Hampton Sandstone|24396|5|Briefly described|p222 Fig.5, p228|Eocene|Eocene|Age: 41-42Ma.  Marine clastics.  Geological Province: Eucla Basin.||||||
25940|Hampton Sandstone|24397|4|Described|p237|||No longer includes Khasta Member (rocks). Overlain by Wilson Bluff Limestone. Geological Province: Eucla Basin.||||||27-JUL-09
25940|Hampton Sandstone|24606|5|Briefly described|p956|Tertiary|Tertiary|Conformably overlain by the Wilson Bluff Limestone. Geological Province: Eucla Basin.||||||
25940|Hampton Sandstone|24617|6|Mentioned|p115 Fig. 3|Eocene|Eocene|Geological Province: Eucla Basin.||||||
25940|Hampton Sandstone|30012|4|Described|Table 1|||||||||
25940|Hampton Sandstone|30268|6|Mentioned|p44|||||||||
25940|Hampton Sandstone|30563|4|Described|p11|||Table on P7||||||
25940|Hampton Sandstone|30564|5|Briefly described|p11|||||||||
25940|Hampton Sandstone|30945|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
25940|Hampton Sandstone|30975|6|Mentioned|Map legend|late Eocene|late Eocene|||||||
25940|Hampton Sandstone|31562|5|Briefly described|p13|||Stratigraphic table P10.||||||
25940|Hampton Sandstone|31850|3|Fully described|p33|||Summary of definition.||||||
25940|Hampton Sandstone|31902|4|Described|Table 1|||Fig.1||||||
25940|Hampton Sandstone|31903|6|Mentioned|Map legend|Tertiary|Tertiary|Section only||||||
25940|Hampton Sandstone|31904|4|Described|p7|||Refers Lowry (1968). See also Table 1||||||
25940|Hampton Sandstone|31906|5|Briefly described|p7|||Refers Lowry (1968). Table 1||||||
25940|Hampton Sandstone|31907|4|Described|p7|||See also Table 1, Fig.1||||||
25940|Hampton Sandstone|31908|4|Described|Table 1|||M.-U.Eocene||||||
25940|Hampton Sandstone|31909|3|Fully described|p7|||Formerly "Hampton Conglomerate".||||||27-JUN-06
25940|Hampton Sandstone|31913|4|Described|Table 1|||P10||||||
25940|Hampton Sandstone|31915|6|Mentioned|Map legend|Eocene|Eocene|||||||
25940|Hampton Sandstone|32117|6|Mentioned|Fig.2|||||||||
25940|Hampton Sandstone|32552|2|Defined|p10|middle Eocene|middle Eocene|See also P11, 37, 53 etc.||||||
25940|Hampton Sandstone|32648|6|Mentioned|p32|||Eocene||||||
25940|Hampton Sandstone|32750|5|Briefly described|p304|||Distribution||||||
25940|Hampton Sandstone|33589|5|Briefly described|p10|||See also P11. U.Eocene.||||||
25940|Hampton Sandstone|33595|6|Mentioned|p6|||||||||
25940|Hampton Sandstone|34192|6|Mentioned|Map legend|Oligocene|Eocene|Lower Miocene - Eocene||||||
25940|Hampton Sandstone|34194|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
25940|Hampton Sandstone|34308|6|Mentioned|Fig.97|||Eocene||||||
25940|Hampton Sandstone|34344|6|Mentioned|p3|||Middle Eocene||||||
25940|Hampton Sandstone|34742|6|Mentioned|Map legend|late Eocene|late Eocene|||||||
25940|Hampton Sandstone|35496|4|Described|Table 1|||Also on P21||||||
25940|Hampton Sandstone|35772|6|Mentioned|p9|||||||||
25940|Hampton Sandstone|36257|6|Mentioned|Table 2.1|||||||||
25940|Hampton Sandstone|36890|3|Fully described|p413|||Formerly Hampton Conglomerate.||||||21-OCT-08
25940|Hampton Sandstone|36902|6|Mentioned|p24|||||||||
25940|Hampton Sandstone|36915|6|Mentioned|Fig.6|||||||||
25940|Hampton Sandstone|38482|6|Mentioned|p24|||See also Table 11.||||||
25940|Hampton Sandstone|39923|6|Mentioned|p354|||||||||
25940|Hampton Sandstone|40003|5|Briefly described|Table 14|||See also Fig.16||||||
25940|Hampton Sandstone|40429|6|Mentioned|Fig.2|||||||||
25940|Hampton Sandstone|41626|6|Mentioned|p46|||||||||
25940|Hampton Sandstone|42086|5|Briefly described|Fig.2 P4|||||||||
25940|Hampton Sandstone|42108|3|Fully described|p323|||||||||
25940|Hampton Sandstone|42265|5|Briefly described|p2|Early Oligocene|Middle Eocene|Terrestrial and marine sequence.||||||13-AUG-08
25940|Hampton Sandstone|42356|5|Briefly described|Fig.15 P119|late Eocene|middle Eocene|See also Microfiche 7 p15, Fig.4, Fig.9, 10, 12, 13.||||||
25940|Hampton Sandstone|42475|6|Mentioned|p20|||||||||
25940|Hampton Sandstone|42535|5|Briefly described|p17|||Eucla Basin||||||
25940|Hampton Sandstone|42545|6|Mentioned|Fig.3 P10|||||||||
25940|Hampton Sandstone|42734|5|Briefly described|map legend|Tertiary||||||||
25940|Hampton Sandstone|42816|3|Fully described|p22|||||||||
25940|Hampton Sandstone|42862|5|Briefly described|p8|||||||||
25940|Hampton Sandstone|42959|5|Briefly described|p57|||see also p58 Fig.3||||||
25940|Hampton Sandstone|43040|5|Briefly described|Fig.2,p861|||||||||
25940|Hampton Sandstone|43053|5|Briefly described|Map Legend|Eocene|Paleocene|Marine sand. Geological Province: Eucla Basin.||||||25-MAY-05
25940|Hampton Sandstone|43065|5|Briefly described|Fig.5,p92|||||||||
25940|Hampton Sandstone|43258|5|Briefly described|Map Legend|Eocene|Paleocene|||||||
25940|Hampton Sandstone|43280|6|Mentioned|Map Legend||Tertiary|||||||
25940|Hampton Sandstone|43298|5|Briefly described|Map Legend|Eocene|Paleocene|||||||
25940|Hampton Sandstone|43498|6|Mentioned|8||Middle Eocene|||||||
25940|Hampton Sandstone|43658|6|Mentioned|p4||Early Eocene|||||||
25940|Hampton Sandstone|43667|6|Mentioned|Fig.3,p12||Middle Eocene|||||||
25940|Hampton Sandstone|43672|5|Briefly described|p330||Early Eocene|||||||
25940|Hampton Sandstone|43813|6|Mentioned|p133|||||||||
25940|Hampton Sandstone|43814|6|Mentioned|Fig.3,p115|||||||||
25940|Hampton Sandstone|43838|4|Described|p4||Tertiary|Interfingers with Pidinga Formation. Princess Royal Spongolite overlies. 35m thick.||||||12-JUL-16
25940|Hampton Sandstone|44133|4|Described|p181|Early Oligocene|Middle Eocene|Geological Province: Eucla Basin. Overlies the Pidinga Formation, Bring Member. Overlain by the Wilson Bluff Limestone. Thickness: 50m. ||||||
25940|Hampton Sandstone|44145|4|Described|p551 Tbl 4-27, p555-6, fig 4-194, p556|Middle Eocene|Middle Eocene|Eucla Basin. Max thickness > 85m. Varied fauna, commonly fragmented.||||Disconformably overlies Madura Formation. Overlain by / grades laterally into lower Wilson Bluff Limestone. Correlated with Pidinga Formation, Werillip Formation.|Limonite-stained sandstone, quartzose, variably calcareous and locally unlithified. Minor conglomerate.|
25940|Hampton Sandstone|44412|14|Not recorded|map legend||Eocene|M.-U.Eocene.||||||
25940|Hampton Sandstone|44695|5|Briefly described|Map Legend|Eocene|Eocene|(Middle-Late Eocene)||||||
25940|Hampton Sandstone|45149|4|Described|p62|||See also P60.||||||
25940|Hampton Sandstone|45168|6|Mentioned|p6|||See also Table 1||||||
25940|Hampton Sandstone|47054|6|Mentioned|p490|||||||||
25940|Hampton Sandstone|49060|6|Mentioned|Fig.5|||||||||
25940|Hampton Sandstone|60953|5|Briefly described|Map Legend|Eocene|Paleocene|Fluvial to esturine and marine sand and lignite. Geological Province: Eucla Basin.||||||27-APR-05
25940|Hampton Sandstone|61108|5|Briefly described|map legend|Eocene|Paleocene|Fluvial to estuarine and marine sand and lignite. Geological Province: Eucla Basin.||||||
25940|Hampton Sandstone|61155|5|Briefly described|p3, p17|Late Eocene|Middle Eocene|Interfingers with Pidinga Formation and Wilson Bluff Limestone, which also overlies this unit in part. Age: 45-36.5Ma. Max. thickness: 50m. Geological Province: Eucla Basin.||||||
25940|Hampton Sandstone|61197|5|Briefly described|p473, p475, p478 Fig.4, p481, p483, p488|Middle Eocene|Middle Eocene|Eucla Basin. Nearshore marine deposits. 0-30m thick. Has dendritic pattern in isopach maps. Probably extends into the Eucla Basin.|||||Medium-very coarse quartz sand; variably calcareous; weakly glauconitic; minor conglomerate.|
25940|Hampton Sandstone|61234|4|Described|p6, p7 Fig. 4|Eocene|Eocene|Overlain by Wilson Bluff Limestone. Geological Province: Eucla Basin. Calcareous, glauconitic and gritty shallow marine. Overlies  Pre-Tertiary rocks.||||||27-JUL-09
25940|Hampton Sandstone|61814|5|Briefly described|p22|Middle Eocene|Middle Eocene|Coarse and fine-grained lignitic and siliciclastic deposit, fluvial and estuarine.||||||08-FEB-10
25940|Hampton Sandstone|61856|5|Briefly described|p300 Fig.2, p304, p313-316  |Middle Eocene|Middle Eocene|Marine. The basal Tertiary unit in the central Eucla Basin.||||Is overlain conformably by Wilson Bluff Limestone.|Shallow marine sandstone, muddy at the base and glauconitic, calcareous and fossiliferous at top; grades upwards into neritic limestones.|22-JAN-15
25940|Hampton Sandstone|62369|5|Briefly described|p409, p410 Fig.4|Late Eocene|Middle Eocene|Estuarine-fluvial to marine deposits. Overlain by Wilson Bluff Limestone. Geological Province: Eucla Basin.||||||
25940|Hampton Sandstone|64340|6|Mentioned|p26 Tb. 5|Late Eocene|Late Eocene|Of Eundynie Group.||||||
25940|Hampton Sandstone|64646|6|Mentioned|p23 Fig. 3, p24 Fig. 4|Eocene||Geological Province: Eucla Basin.||||||08-FEB-10
25940|Hampton Sandstone|65194|5|Briefly described|p31, p136 Fig.4.37, p141, p164, p170|Late Eocene|Middle Eocene|Partially silicified fine- to medium-grained sand. Marine sediments in Gawler Craton and Lefroy Palaeovalley which interfinger with Pidinga Formation. High groundwater salinity. Correlated with the Wollubar Sandstone.||||||08-APR-16
25940|Hampton Sandstone|65260|6|Mentioned|p26-27, p27 Fig.20|Late Eocene||Of Eundynie Group. Interfingers with the Princess Royal Member in the Lefroy Palaeochannel. Fine-grained to gravelly glauconitic sand, locally weakly cemented to sandstone. Contains marine fauna, most commonly siliceous sponge spicules. Proposed by Clarke et al. (2003) to be subsumed into Pallinup Formation.||||||
25940|Hampton Sandstone|65891|6|Mentioned|p221 Fig.5. |Paleogene|Paleogene|East Eucla Basin. Lutetian age.||||||
25940|Hampton Sandstone|65942|2|Defined|p75|Middle Eocene|Middle Eocene|||Eucla Group||||28-MAY-10
25940|Hampton Sandstone|66131|6|Mentioned|p242 Fig.2|Eocene|Eocene|Middle-Late Eocene in age (from p.242 Fig.2 - stratigraphic correlation chart).||||||
25940|Hampton Sandstone|67462|5|Briefly described|Map legend.|Eocene|Eocene|Bunda Plateau, Eucla Basin.||||||
25940|Hampton Sandstone|67921|5|Briefly described|Map legend|Eocene|Eocene|Occurs as a sheet beneath and between Ooldea, Barton and Paling Ranges.|||||Marine and non-marine quartz sand. Varicoloured, in part silicified and ferruginised.|
25940|Hampton Sandstone|68715|6|Mentioned|p30 Fig.5|Eocene|Eocene|Bunda Plateau, Eucla Basin. Middle Eocene age.||||||
25940|Hampton Sandstone|69598|5|Briefly described|p2, p9, p11 Tb.1, p29 Tb.4|Middle Eocene|Middle Eocene|Eucla Basin. Up to 85m thick. Potential carbon dioxide storage reservoir. Deposited in a shallow marine environment. ||Eundynie Group|||Spicular and calcareous sandstones.|
25940|Hampton Sandstone|69632|5|Briefly described|p26, p30|Eocene|Eocene|Eucla Basin.||||Overlies Madura Formation. Is overlain by Wilson's Bluff Formation.|A lenticular sandstone unit.|
25940|Hampton Sandstone|69648|4|Described|p4, p21-22, p25, p29, p36-37, map legend|Eocene|Eocene|Eucla Basin. Hampton Sandstone, Ooldea Sand, Yarle Sandstone are source of sand for Tertiary coastal sand units (including Wintrena Formation). Thickness: ~25-45m. No diagnostic fossils for age determination. Prospective for heavy mineral sand deposits. Low level mineralisation (best value was 8.37% heavy minerals in M169 28-30 m, EL 1654). Unclear in text: interbedded with/overlying? Wilson Bluff Limestone. Age: Middle to Late Eocene.||Burdunga Subgroup||With Ooldea Sand, overlies Pidinga Formation; conformably overlain by Paling Member (Wilson Bluff Limestone); unconformably overlain by Garford Formation.|Terrigenous clastic sediments; siliciclastic sands of marine and coastal origin; rare, minor clay horizons.|
25940|Hampton Sandstone|69649|5|Briefly described|p31, p32, p58|Eocene|Eocene|Eucla Basin. Represents a major marine transgression during Middle Eocene.|||||A sheet of very fine to coarse sand and grit, including heavy minerals, reworked by wave action into strandlines. Silcrete surface.|
25940|Hampton Sandstone|70397|5|Briefly described|p3|Middle Eocene|Middle Eocene|Eucla Basin.||Unit of Eucla Group.||Overlain by Wilson Bluff Limestone. Unconformably underlain by Madura Formation.||29-JUL-19
25940|Hampton Sandstone|70771|5|Briefly described|p27|||Eucla Basin.||||Unconformably overlies the Madura Formation.||
25940|Hampton Sandstone|70772|6|Mentioned|p2, p6-p7, p14, p22, p31, p38, p41|Eocene|Eocene|Bight Basin. Hosts possible microtektites.||||Unconformably overlies the Madura Formation.||
25940|Hampton Sandstone|70778|5|Briefly described|p4|||Intersected in Nundroo 3 DDH.|||||Clayey-sand.|
25940|Hampton Sandstone|71361|5|Briefly described|p5, p12|Middle Eocene|Middle Eocene|Eucla Basin. Interpreted to have been deposited when the Eucla Basin was flooded by the Southern Ocean.|c. 43 Ma|||Unconformably overlies the Madura Formation. Overlain by the Wilson Bluff Limestone.||
25940|Hampton Sandstone|71618|6|Mentioned|p124-125,127|Cenozoic|Cenozoic|Geological province: Eucla Basin.||||Disconformably overlies Madura Formation.||05-SEP-19
25940|Hampton Sandstone|71891|5|Briefly described|p6-p7|Cenozoic|Cenozoic|Eucla Basin, Coompana Province. 20-60m thick. Intepreted to have been deposited in marine, estuarine and fluvial environments.||||Overlies the Pidinga Formation. Overlain by the Wilsons Bluff Limestone.|Quartz-rich sandstone, carbonaceous sandstone.|12-MAY-23
25940|Hampton Sandstone|72344|5|Briefly described|p4|||Eucla Basin. Deposited as lenses and sheets in marine, estuarine and fluvial environments. See also p160.||||Overlies the Pidinga Formation. Overlain by the Wilson Bluff Limestone.|Poorly sorted limonite stained sandstone, typically quartz rich; includes subordinate gravel, conglomerate and siltstone.|
25940|Hampton Sandstone|72465|5|Briefly described|p9|Tertiary|Tertiary|Eucla Basin, Coompana Province. Deposited as lenses and sheets in marine, estuarine and fluvial environments.||||Overlies Pidinga Formation. Is overlain by Wilson Bluff Limestone.|Poorly-sorted limonite-stained sandstone, typically quartz-rich; includes subordinate gravel, conglomerate and siltstone.|
25940|Hampton Sandstone|72466|5|Briefly described|p9|Tertiary|Tertiary|Benbow et al. (1995). Eucla Basin, Coompana Province. Deposited as lenses and sheets in marine, estuarine and fluvial environments.||||Overlies Pidinga Formation. Is overlain by the Wilson Bluff Limestone.|Poorly-sorted limonite-stained sandstone, typically quartz-rich; includes subordinate gravel, conglomerate and siltstone.|
25940|Hampton Sandstone|72467|5|Briefly described|p9|Tertiary|Tertiary|Eucla Basin, Coompana Province. Deposited as lenses and sheets in marine, estuarine and fluvial environments.||||Overlies Pidinga Formation. Is overlain by Wilson Bluff Limestone.|Poorly-sorted limonite-stained sandstone, typically quartz-rich; includes subordinate gravel, conglomerate and siltstone.|
25940|Hampton Sandstone|72468|5|Briefly described|p9|||Eucla Basin. Deposited in marine, estuarine and fluvial environments.||||Underlain by Pidinga Formation. Overlain by Wilson Bluff Limestone.|Poorly sorted limonite-stained sandstone, typically quartz rich; includes subordinate gravel, conglomerate and siltstone.|
25940|Hampton Sandstone|72469|5|Briefly described|p9|||Eucla Basin. Deposited in marine, estuarine and fluvial environments.||||Underlain by Pidinga Formation. Overlain by Wilson Bluff Limestone.|Poorly sorted limonite-stained sandstone, typically quartz rich; includes subordinate gravel, conglomerate and siltstone.|
25940|Hampton Sandstone|72470|5|Briefly described|p9|||Eucla Basin. Deposited in marine, estuarine and fluvial environments.||||Underlain by Pidinga Formation. Overlain by Wilson Bluff Limestone.|Poorly sorted limonite-stained sandstone, typically quartz rich; includes subordinate gravel, conglomerate and siltstone.|
25940|Hampton Sandstone|72471|5|Briefly described|p9|||Eucla Basin. Deposited in marine, estuarine and fluvial environments.||||Underlain by Pidinga Formation. Overlain by Wilson Bluff Limestone.|Poorly sorted limonite-stained sandstone, typically quartz rich; includes subordinate gravel, conglomerate and siltstone.|
25940|Hampton Sandstone|72472|5|Briefly described|p9|||Eucla Basin. Deposited in marine, estuarine and fluvial environments.||||Underlain by Pidinga Formation. Overlain by Wilson Bluff Limestone.|Poorly sorted limonite-stained sandstone, typically quartz rich; includes subordinate gravel, conglomerate and siltstone.|
25940|Hampton Sandstone|73084|5|Briefly described|p16-17|Eocene|Eocene|Up to 20 m thick[?].||||Unconformably[?] underlain by Madura Formation. Overlain by Wilson Bluff Limestone.|Carbonaceous sandstone.|
25940|Hampton Sandstone|73111|5|Briefly described|Map legend.|Pleistocene|Eocene|Is overlain by un-named indurated, red-brown to orange calcareous aeolian sand.||||||
25940|Hampton Sandstone|73641|5|Briefly described|p5|Eocene|Eocene|Eucla Basin. <25m thick. Marine, estuarine and fluvial deposits.||||Overlies Pidinga Formation. Is overlain by Wilson Bluff Limestone.|Typically poorly sorted, limonite-stained, and quartz-rich sandstone; subordinate conglomerate and siltstone.|
24309|Heysen Supergroup|22772|5|Briefly described|p63,Table13.1|Neoproterozoic III|Cryogenian|Includes: Umberatana and Wilpena Groups.||||||
24309|Heysen Supergroup|22857|5|Briefly described|p63, Tb. 13.1 (insert p70-71)|Marinoan|Sturtian|Comprises the Wilpena and Umberatana Groups. Age: 700-545Ma.||||||
24309|Heysen Supergroup|23516|5|Briefly described|p599 Fig.5|Neoproterozoic|Neoproterozoic|||||||
24309|Heysen Supergroup|24586|5|Briefly described|p51 Fig. 1|Adelaidean|Adelaidean|Includes Wilpena, Umberatana, Burra and Callanna Groups. Geological Province: Adelaide Geosyncline.||||||
24309|Heysen Supergroup|38004|2|Defined|p82|Precambrian|Precambrian|||||||
24309|Heysen Supergroup|38703|6|Mentioned|p131|||||||||
24309|Heysen Supergroup|38704|6|Mentioned|p133|||||||||
24309|Heysen Supergroup|39344|6|Mentioned|Map legend|Precambrian|Adelaidean|Sturtian to Marinoan||||||
24309|Heysen Supergroup|40763|6|Mentioned|p204|||||||||
24309|Heysen Supergroup|41364|6|Mentioned|Fig.1|||||||||
24309|Heysen Supergroup|41401|5|Briefly described|p32|||||||||
24309|Heysen Supergroup|41647|6|Mentioned|Fig.2|||||||||
24309|Heysen Supergroup|41770|6|Mentioned|Fig.1|||||||||
24309|Heysen Supergroup|42011|6|Mentioned|Fig.2 P457|||||||||
24309|Heysen Supergroup|42028|6|Mentioned|p137|||||||||
24309|Heysen Supergroup|42215|6|Mentioned|Fig.2 P448|||||||||
24309|Heysen Supergroup|42238|6|Mentioned|p73|||||||||
24309|Heysen Supergroup|42239|6|Mentioned|Fig.2 P151|||||||||
24309|Heysen Supergroup|42882|5|Briefly described|Table 1 P3|||||||||
24309|Heysen Supergroup|43052|6|Mentioned|p172|||||||||
24309|Heysen Supergroup|43595|5|Briefly described|p543-545||Neoproterozoic|||||||
24309|Heysen Supergroup|43845|5|Briefly described|Fig2 p42||Neoproterozoic|||||||12-JUL-16
24309|Heysen Supergroup|60959|5|Briefly described|Map Legend|Adelaidean|Adelaidean|||||||
24309|Heysen Supergroup|62592|5|Briefly described|p50 Table 5.1.|Ediacaran|Sturtian|Adelaide Geosyncline.|||Includes Umberatana and Wilpena Groups.|Unconformably overlies Warrina Supergroup. Is overlain disconformably by Moralana Supergroup.||23-JAN-19
24309|Heysen Supergroup|62664|6|Mentioned|p138 Fig.2.|Neoproterozoic|Neoproterozoic||||Includes Umberatana and Wilpena Groups.|||
24309|Heysen Supergroup|64801|6|Mentioned|p110-111|Neoproterozoic|Neoproterozoic|Passive margin phase of deposition.|||Umberatana, Wilpena Groups.|Overlies Warrina Supergroup. Is overlain by Moralana Supergroup.||
24309|Heysen Supergroup|65376|6|Mentioned|p9 Fig.1.2. |Neoproterozoic|Neoproterozoic||||||Largely marine sediments including glacial sediments to base.|
24309|Heysen Supergroup|66884|6|Mentioned|p41 Fig.3||||||Umberatana Group|||
24309|Heysen Supergroup|68030|6|Mentioned|p236,238|Ediacaran|Cryogenian|Flinders Ranges.|||Includes Wilpena and Umberatana groups.|Overlies the Warrina Supergroup.||26-JUN-19
24309|Heysen Supergroup|68131|5|Briefly described|p2 Fig.1|Neoproterozoic|Neoproterozoic|Largely marine sediments with glacial sediments at base.||||||
24309|Heysen Supergroup|70384|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Adelaide Geosyncline. Age shown more specifically as Sturtian [Cryogenian] to Ediacaran.|||Includes Umberatana, Wilpena Groups.|||23-JAN-19
24309|Heysen Supergroup|70407|5|Briefly described|p102 Fig 1, p103 Fig 2|Neoproterozoic|Neoproterozoic|Age: Sturtian - Marinoan|||Includes Umberatana Group, Wilpena Group.|||
24309|Heysen Supergroup|71593|4|Described|p19-p20|Neoproterozoic|Neoproterozoic|Gawler Craton. Related to the latter stages of Rodinia breakup and formation of the Adelaide Rift System.|700-545 Ma|||Overlies the Warrina Supergroup. Unconformably overlain by the Normanville Group.|Glaciogenic, shale, carbonate and quartzite sediments and related igneous rocks.|
24309|Heysen Supergroup|72601|6|Mentioned|p5||||||Tapley Hill Formation, Balcanoona Formation, Wockerawirra Dolomite, Enorama Shale, Wundowie Limestone Member, Tindelpina Shale Member, Umberatana Group|||
24309|Heysen Supergroup|73086|6|Mentioned|p72, p161|||Adelaide Rift Complex.|||Wockerwirra Member, Tapley Hill Formation, Umbertana Subgroup|Partly correlates to Aralka Formation.||
24309|Heysen Supergroup|73222|6|Mentioned|p6|Ediacaran|Tonian|Adelaide Rift Complex.|||Umberatana Group, Wilpena Group, and units therein|||
24309|Heysen Supergroup|73236|6|Mentioned|p35, p38||||||Umberatana Group, Wilpena Group, and units therein|||
24309|Heysen Supergroup|73262|6|Mentioned|p583|[Cryogenian?]|[Ediacaran?]||||Umberatana Group, Wilpena Group|||
24309|Heysen Supergroup|74367|5|Briefly described|p4, p6, p19|Ediacaran|Cryogenian|Considered to represent period of thermal sag. Absolute minimum age of deposition from Heatherdale Shale (514.98+/-0.22 Ma; Betts et al., 2018).|||Umberatana Group, Wilpena Group|||
73300|Heytesbury Supersequence|63134|2|Defined|112|||||||||
73300|Heytesbury Supersequence|63269|5|Briefly described|p605|Miocene|Oligocene|Otway Basin.||||Overlies Nirranda Supersequence. Is overlain by Whalers Bluff Supersequence.||
73300|Heytesbury Supersequence|69297|6|Mentioned|p80, p110, p111|||||||||
73300|Heytesbury Supersequence|69651|5|Briefly described|p10, p12-15, p17-19, p22-23, p29, p39|Miocene|Oligocene|See also p44-47, p49-50. Open marine deposits. Possible seals. Modelling diagrams.||||Overlies Nirranda Supersequence. Is overlain by Whalers Bluff Supersequence.|Calcareous claystone overlain by marls, calcarenite and calcilutite; shaly limestone overlain by calcarenite and calcilutite; quartz sandstone overlain by silty mudstone, and limestone.|
73300|Heytesbury Supersequence|70077|5|Briefly described|Regional: Fig.4; p4-5|Miocene|Oligocene|Otway Basin.||||Overlies Nirranda Supersequence. Is overlain by Whalers Bluff Supersequence.||
73300|Heytesbury Supersequence|70078|5|Briefly described|Regional: Fig.4; p3|Miocene|Oligocene|||||Unconformably overlies Nirranda Supersequence. Is overlain by Whalers Bluff Supersequence.|Shelfal marls and limestones.|
73300|Heytesbury Supersequence|70880|5|Briefly described|p77|Miocene|Oligocene|Otway Basin. Open marine environment.||||Overlies Nirranda Supersequence. Is overlain by Whalers Bluff Supersequence.|Mixed carbonate/siliciclastic sediments.|
73300|Heytesbury Supersequence|71266|5|Briefly described|p614 Fig.3, p615|Miocene|Oligocene|Otway Basin.||||Overlies Nirranda Supersequence. Is overlain by Whalers Bluff Supersequence.||
27273|Hideaway Well Member|40431|2|Defined|p14|Early Cambrian|Early Cambrian|Atdabanian||||||
27273|Hideaway Well Member|42233|4|Described|p249|||||||||
27273|Hideaway Well Member|44133|5|Briefly described|p22|||Of the Wilkawillina Limestone.||||||
27273|Hideaway Well Member|69570|5|Briefly described|p420, p422-p425, p428|||A new Taxon, J. phaseloa sp. Nov., has a first appearance in shallow water facies of this unit. Contact with the Winnitinny Creek Member has been described as disconformable in the type area at Bunkers Range but is not apparent in this study.||Wilkawillina Limestone||Overlies the Mount Mantell Member. Overlain by the Winnitinny Creek Member.|Biohermal carbonates.|
27273|Hideaway Well Member|70833|5|Briefly described|p180,183-188,190-192,194,201,203|Terreneuvian|Terreneuvian|Of Arrowie Basin. Key sections: MORO (S of Moro Gorge, Arrowie Syncline); BALC (Balcoracana Gorge, Bunkers Range); MMT (Bunkers Range, central Flinders Ranges); WILK (Bunkers Graben); 10MS-W (Ten Mile South, SE Bunkers Graben). Characterised by increased abundance of archaeocyaths, both fragmentary and in situ, and relatively large bioherms are commonly developed. Deposited in a high-energy, shallow water carbonate environment. Includes K. rostana zone. Correlable to Fork Tree Limestone in the Stansbury Basin.||Unit of Wilkawillina Limestone.||Conformably overlain by Winnitinny Creek Member. Underlain by Mount Mantell Member. Interfingers with Wirrapowie Limestone north of Wirrealpa hinge Zone.||08-AUG-19
27273|Hideaway Well Member|70835|6|Mentioned|p336|Cambrian|Cambrian|Arrowie Basin, Flinders Ranges.||Wilkawillina Limestone.||Overlies Mount Mantell Member. Is overlain by Winnitinny Creek Member.||
27273|Hideaway Well Member|71102|5|Briefly described|p267|Terreneuvian|Terreneuvian|Of Arrowie Basin.||||Overlain by Winnitinny Creek Member. Underlain by Mount Mantell Member.||
26613|Hiltaba Suite|22494|5|Briefly described|p35|Calymmian|Calymmian|||||||
26613|Hiltaba Suite|22613|5|Briefly described|p14|||||||||
26613|Hiltaba Suite|22614|5|Briefly described|map|Mesoproterozoic|Mesoproterozoic|||||||
26613|Hiltaba Suite|22629|4|Described|fig2, p147,152,158|Calymmian|Calymmian|Age: 1600-1585 Ma.||||||18-JAN-07
26613|Hiltaba Suite|22631|6|Mentioned|p173|Calymmian|Calymmian|1595 Ma.||||||28-OCT-22
26613|Hiltaba Suite|22771|6|Mentioned|p36,Map2p34-35,50||Calymmian|Max Age: ~1500 Ma.||||||
26613|Hiltaba Suite|22857|4|Described|p36, p50, p396 App.1 Tb.A1.2|Mesoproterozoic|Mesoproterozoic|Two-mica granite, adamellite, muscovite pegmatite. Age: 1490+/-20Ma (Rb/Sr, Pidgeon 1967 and Harrison and McDougall 1981). Geological Province: Gawler and Curnamona Cratons.||||||
26613|Hiltaba Suite|22873|6|Mentioned|P9|||||||||
26613|Hiltaba Suite|22916|6|Mentioned|12|||||||||
26613|Hiltaba Suite|22918|6|Mentioned|50|||||||||
26613|Hiltaba Suite|22933|6|Mentioned|Fig11.9p15,21|||||||||
26613|Hiltaba Suite|22950|6|Mentioned|p47|||||||||
26613|Hiltaba Suite|23054|6|Mentioned|p33||Mesoproterozoic|||||||
26613|Hiltaba Suite|23123|5|Briefly described|p403||Mesoproterozoic|||||||
26613|Hiltaba Suite|23175|6|Mentioned|p5||Mesoproterozoic|||||||
26613|Hiltaba Suite|23204|6|Mentioned|p1363|||||||||
26613|Hiltaba Suite|23342|5|Briefly described|28 Fig.1|Mesoproterozoic|Mesoproterozoic|||||||
26613|Hiltaba Suite|23386|6|Mentioned|p22|||Geological Province: Gawler Craton||||||
26613|Hiltaba Suite|23396|6|Mentioned|p426|||||||||
26613|Hiltaba Suite|23479|5|Briefly described|p26|Mesoproterozoic|Mesoproterozoic|Geological Province: Gawler Craton.||||||
26613|Hiltaba Suite|23480|5|Briefly described|p21|Mesoproterozoic|Paleoproterozoic|Age: ~1600-1585 Ma. See also p20 Fig 1.||||||07-NOV-08
26613|Hiltaba Suite|23481|5|Briefly described|p19 Fig 1|||See also p18. Geological Province: Gawler Craton.||||||
26613|Hiltaba Suite|23719|5|Briefly described|p23|Mesoproterozoic|Mesoproterozoic|Geological Province: Gawler Craton.||||||
26613|Hiltaba Suite|23803|5|Briefly described|p28 Fig. 2|Paleoproterozoic|Paleoproterozoic|Age: 1598-1580Ma. Geological Province: Gawler Craton.||||||07-NOV-08
26613|Hiltaba Suite|23805|5|Briefly described|p4 Fig. 1|Mesoproterozoic|Mesoproterozoic|Geological Province: Gawler Craton.||||||
26613|Hiltaba Suite|23907|5|Briefly described|p5|Mesoproterozoic|Mesoproterozoic|Geological Province: Mount Woods Inlier.||||||
26613|Hiltaba Suite|23957|6|Mentioned|p1127|||||||||
26613|Hiltaba Suite|24197|4|Described|p8, p30|||Divided into 2 types: Roxby Downs type (granite, syenogranite, qtz monzodiorite, qtz monzonite, syenite, aplite, mozogranite, leucotonalite): Kokatha type (syenite, granodiorite, monzogranite, granite). Geol.prov: Gawler Craton. Type eg.of Hiltaba Assoc.||||||07-FEB-11
26613|Hiltaba Suite|24217|5|Briefly described|p832 Fig. 1|Proterozoic|Proterozoic|Geological Province: Gawler Craton.||||||21-OCT-08
26613|Hiltaba Suite|24261|4|Described|p1046|Mesoproterozoic|Mesoproterozoic|Geological Province: Gawler Craton.||||||21-OCT-08
26613|Hiltaba Suite|24285|5|Briefly described|p24|Mesoproterozoic|Mesoproterozoic|||||||
26613|Hiltaba Suite|24296|5|Briefly described|p1251 Fig. 2|Mesoproterozoic|Mesoproterozoic|Age: 1590 Ma. Geological Province: Gawler Craton.||||||
26613|Hiltaba Suite|24346|5|Briefly described|p98|Mesoproterozoic|Mesoproterozoic|Age: ca. 1600 - ca. 1588Ma (U-Pb zircon, Flint 1993).||||||18-JAN-07
26613|Hiltaba Suite|24356|5|Briefly described|p1593|Mesoproterozoic|Mesoproterozoic|Granites. Comagmatic with Gawler Range Volcanics.  Age: 1600-1585Ma. Geological Province: Gawler Craton.||||||15-SEP-05
26613|Hiltaba Suite|24365|6|Mentioned|p5 Fig.2|||||||||
26613|Hiltaba Suite|24381|6|Mentioned|p58|||||||||
26613|Hiltaba Suite|24472|5|Briefly described|p5 Tb.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Harris Greenstone Domain, Gawler Craton. Age: ~1590 Ma.||||||21-OCT-08
26613|Hiltaba Suite|24475|5|Briefly described|p46, p49 Tb.1|Mesoproterozoic|Mesoproterozoic|||||||
26613|Hiltaba Suite|24505|5|Briefly described|p6, p5 Fig. 1|Mesoproterozoic|Mesoproterozoic|Age: ~1595-1575Ma.  Geological Province: Gawler Craton.||||||15-SEP-05
26613|Hiltaba Suite|24526|5|Briefly described|p97 Fig. 3, p100|Paleoproterozoic|Paleoproterozoic|Age: 1620-1550Ma.  Geological Province: Gawler Craton.  See also p96 Fig. 3.||||||07-NOV-08
26613|Hiltaba Suite|24583|6|Mentioned|p12|||||||||
26613|Hiltaba Suite|39349|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
26613|Hiltaba Suite|40430|6|Mentioned|Table 2|||||||||
26613|Hiltaba Suite|40448|5|Briefly described|p35 Table 4||||1445+/-39Ma, 1556+/-30Ma etc||Includes Charleston Granite.|Intrudes Gawler Range Volcanics, Corunna Conglomerate. Intruded by rhyolite dykes in Nuyts Archipelago.||
26613|Hiltaba Suite|40644|6|Mentioned|p121, p124 Fig. 3|Mesoproterozoic|Mesoproterozoic|Includes the Charleston Granite. See also Hiltaba Suite granitoids in Fig. 2, p120.||||||13-AUG-08
26613|Hiltaba Suite|40941|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
26613|Hiltaba Suite|41327|6|Mentioned|Fig.1|||||||||
26613|Hiltaba Suite|41402|6|Mentioned|p35|||||||||
26613|Hiltaba Suite|41493|6|Mentioned|Table 1|||||||||
26613|Hiltaba Suite|41619|6|Mentioned|Map legend|Mesoproterozoic||||||||
26613|Hiltaba Suite|41667|6|Mentioned|Fig.2|||||||||
26613|Hiltaba Suite|41995|6|Mentioned|Fig.1 p13|||||||||28-OCT-22
26613|Hiltaba Suite|42167|6|Mentioned|Fig.4 p117|||||||||28-OCT-22
26613|Hiltaba Suite|42291|6|Mentioned|Fig.1 P3|||||||||
26613|Hiltaba Suite|42357|6|Mentioned|p8|||||||||
26613|Hiltaba Suite|42465|5|Briefly described|Map Legend|||||||||
26613|Hiltaba Suite|42466|5|Briefly described|Map Legend|||||||||
26613|Hiltaba Suite|42468|5|Briefly described|Fig. 1 P2|||||||||
26613|Hiltaba Suite|42469|4|Described|p19|||||||||
26613|Hiltaba Suite|42470|6|Mentioned|Fig.1 P18|||||||||
26613|Hiltaba Suite|42475|4|Described|p17|||||||||
26613|Hiltaba Suite|42546|5|Briefly described|Map legend|Mesoproterozoic||||||||
26613|Hiltaba Suite|42716|5|Briefly described|Map legend|Mesoproterozoic||||||||
26613|Hiltaba Suite|42736|5|Briefly described|map legend|Mesoproterozoic||||||||
26613|Hiltaba Suite|42738|5|Briefly described|map legend|Mesoproterozoic||||||||
26613|Hiltaba Suite|43049|5|Briefly described|p14|||||||||
26613|Hiltaba Suite|43052|3|Fully described|p127|||see also Table 5.6||||||
26613|Hiltaba Suite|43053|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Anorogenic granitoids. Includes Charleston Granite, Tickera Granite, and Arthurton Granite (Gawler Craton), and Balta Granite (Mount Woods Inlier), and equivalents within the Willyama Inlier.||||||26-MAY-05
26613|Hiltaba Suite|43258|5|Briefly described|Map Legend||Mesoproterozoic|||||||
26613|Hiltaba Suite|43298|6|Mentioned|Map Legend||Mesoproterozoic|||||||
26613|Hiltaba Suite|43595|5|Briefly described|p443|||||||||
26613|Hiltaba Suite|43621|6|Mentioned|p27|||granites||||||
26613|Hiltaba Suite|43839|5|Briefly described|p29-30||Mesoproterozoic|In Gawler Craton||||||12-JUL-16
26613|Hiltaba Suite|44194|6|Mentioned|p1|||||||||
26613|Hiltaba Suite|44695|5|Briefly described|Map Legend||Mesoproterozoic|||||||
26613|Hiltaba Suite|44935|5|Briefly described|Map Legend||Proterozoic|||||||
26613|Hiltaba Suite|50081|6|Mentioned|p42|||||||||
26613|Hiltaba Suite|60484|5|Briefly described|p33 Fig. 1|Calymmian|Calymmian|Age: 1595-1575Ma.  Geological Province: Gawler Craton.  See also p38.||||||
26613|Hiltaba Suite|60496|5|Briefly described|p23|||Intrudes the Gawler Range Volcanics.||||||
26613|Hiltaba Suite|60515|5|Briefly described|p115, p116 Fig.1, p122 Tb.1|||Gawler Craton.|c.1600-1580 Ma.|||||
26613|Hiltaba Suite|60704|5|Briefly described|p685, p686 Fig.1|Mesoproterozoic|Mesoproterozoic|Age: ca. 1590 Ma. Geological Province: Gawler Craton.||||||11-APR-05
26613|Hiltaba Suite|60707|5|Briefly described|p611|||Includes the Calca Granite.||||||
26613|Hiltaba Suite|60900|6|Mentioned|p897|Mesoproterozoic|Mesoproterozoic|In South Australia.||||||
26613|Hiltaba Suite|60953|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Age: 1598-1575Ma.||||||
26613|Hiltaba Suite|60954|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Plutons, sheets and granitoids. Geological Province: Gawler Craton.||||||31-MAY-05
26613|Hiltaba Suite|60958|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Granitoid intrusives. Age: ~1600-1580Ma. Geological Province: Gawler Craton.||||||
26613|Hiltaba Suite|61108|5|Briefly described|map legend|Mesoproterozoic|Mesoproterozoic|Includes Charleston Granite, Tickera Granite and Balta Granite. Dominantly anorogenic granite to adamellite; lesser quartz monzodiorite, quartz monzonite and granodiorite. Age: 1598-1575 Ma.||||||
26613|Hiltaba Suite|61121|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Granitoid intrusives.  Age: ~1600-~1580Ma. Geological Province: Gawler Craton.||||||
26613|Hiltaba Suite|61154|5|Briefly described|p36|Mesoproterozoic|Mesoproterozoic|Hosts the Olympic Dam ore body. Age: 1595-1585Ma. Geological Province: Gawler Craton.||||||23-JUL-13
26613|Hiltaba Suite|61262|5|Briefly described|p445 Fig. 1|Mesoproterozoic|Paleoproterozoic|Geological Province: Gawler Craton.||||||07-NOV-08
26613|Hiltaba Suite|61307|5|Briefly described|p36 Fig. 17|Mesoproterozoic|Mesoproterozoic|Age: ~1585Ma. Geological Province: Gawler Craton. See also p39 Fig. 19.||||||
26613|Hiltaba Suite|61393|5|Briefly described|p164, p166 Fig.1, p167, p175.   |Mesoproterozoic|Mesoproterozoic|Eastern and Central Gawler Craton. Voluminous felsic, and subordinate mafic, magmatic rocks.|c.1595 - 1575 Ma.||||Sheared granites and granodiorites.|
26613|Hiltaba Suite|61522|5|Briefly described|p4|Mesoproterozoic|Mesoproterozoic|Geological Province: Gawler Craton.||||||
26613|Hiltaba Suite|61565|5|Briefly described|p???|||Granites.   Geological Province: Gawler Craton.||||||20-APR-06
26613|Hiltaba Suite|61659|4|Described|p30 Fig.1, p31, pp37-41.   |Mesoproterozoic|Mesoproterozoic|Gawler Craton. Co-magmatic with Gawler Range Volcanics. Cross-cut by re-activated Tallacootra Shear Zone and Coorabie Fault Zone c. 1515 - 1500 and 1470 - 1455 Ma; these are in turn truncated by the younger Karari Fault Zone. S.G. = 2.63 +/- 0.05.|1589-1578 Ma (Daly et al. 1998).|||Intrudes the Mulgathing Complex and Muckanippie Anorthosite Complex.||
26613|Hiltaba Suite|61733|6|Mentioned|p57|||Gawler Craton. Emplacement age.|c.1590-1575 Ma|||||
26613|Hiltaba Suite|61735|6|Mentioned|p654|||In S.A.||||||30-JUN-09
26613|Hiltaba Suite|61736|6|Mentioned|p664|||Geological province: Gawler Craton.||||||
26613|Hiltaba Suite|61864|5|Briefly described|p16 fig 3, p17|||Mildly deformed plutons.||||||
26613|Hiltaba Suite|62535|6|Mentioned|p664|||Gawler Craton.||||||
26613|Hiltaba Suite|62536|5|Briefly described|p654|||Likely synchronous with magmatism in the Broken Hill area.|~1600 Ma.||||Felsic magmatism.|
26613|Hiltaba Suite|62592|6|Mentioned|pp74.|||Gawler Craton. Coeval with Hiltaba Suite plutons.||||||
26613|Hiltaba Suite|62641|6|Mentioned|p277 Fig.1. ||||1.59-1.57 Ga.|||||
26613|Hiltaba Suite|62893|4|Described|Map Legend, p15-16, p25, p28-29, p41|Middle Proterozoic|Middle Proterozoic|Represents a large volume, high-level, anorogenic magmatic event. Associated with pronounced gravity lows where it is exposed or shallowly concealed. Ages of 1477 +/- 34 Ma (Rb-Sr) and 1519 +/- 67 Ma (Rb-Sr) have previously been reported. Two major varieties of granite are represented on the Kimba mapsheet.||||Equivalent to Gawler Range Volcanics.|Massive, coarse-grained and phenocrystic, pink-red granite and adamellite with veins of pegmatite and aplite, and large, pink K-feldspar phenocrysts and white-green plagioclase.|
26613|Hiltaba Suite|62978|5|Briefly described|p161, p165|Mesoproterozoic|Mesoproterozoic|Associated with the Gawler Range Volcanics. Age: ~1590Ma. Geological Province: Gawler Craton.||||||07-FEB-11
26613|Hiltaba Suite|63020|5|Briefly described|p987 Fig. 8|Mesoproterozoic|Mesoproterozoic|Age: ~1590Ma. Geological Province: Gawler Craton.||||||10-AUG-07
26613|Hiltaba Suite|63102|5|Briefly described|p42|||Geological province: Gawler Craton. Temporally equivalent to Bimbowrie Supersuite.||||||
26613|Hiltaba Suite|63223|5|Briefly described|p16, p17 Fig. 1|Mesoproterozoic|Mesoproterozoic|Geological Province: Gawler Craton.||||||30-APR-07
26613|Hiltaba Suite|63224|6|Mentioned|p10|||Geological Province: Gawler Craton.||||||07-FEB-08
26613|Hiltaba Suite|63275|6|Mentioned|p13, p14 Fig.1, p18.|Early Mesoproterozoic|Early Mesoproterozoic||||||Granitoids.|
26613|Hiltaba Suite|63398|5|Briefly described|p661, p663|Mesoproterozoic|Mesoproterozoic|Includes Tickera and Arthurton Granites. Historically, the granites of this suite have been divided into Tickera Granite north of Moonta and Arthurton Granite south of Moonta. Age: 1600-1580Ma. Geological Province: Gawler Craton. See also p667.||||||10-DEC-07
26613|Hiltaba Suite|63776|6|Mentioned|p1089|||Geological Province: Gawler Craton.||||||17-MAR-09
26613|Hiltaba Suite|63866|5|Briefly described|p3, p7, p13, p18-p21, p32|Mesoproterozoic|Mesoproterozoic|Associated with mineralisation in the gawler craton and comprises extensive gold-onlu and IOCG+U mineralisation. U-Pb ages from granites of this suite in the Nuyts Domain are dated at 1596+/- 9 Ma and 1562 +/- 16 Ma.|ca. 1600-1575 Ma||Includes the Calca Granite.|||
26613|Hiltaba Suite|64130|4|Described|p1377, p1378 Fig.1, p1380 Fig.2    |Mesoproterozoic|Mesoproterozoic|See also p1383, p1387-1393. Comagmatic with Gawler Range Volcanics. Emplacement coincided with the major mineralising interval in the Gawler Craton. Mostly intruded as lopolitic upper crustal plutons. May be two phases of magmatism, one at ca.1590 Ma and one at ca.1580 Ma |1595-1575 Ma.|||Comagmatic with the Gawler Range Volcanics|Predominantly highly fractionated granite to granodiorite with minor mafic rocks.|
26613|Hiltaba Suite|64131|5|Briefly described|p1397, p1399 Fig.2, p1400-1410|||High-level sill-like intrusions emplaced immediately prior to IOCG mineralisation. Petrophysical properties.|~1595-1575 Ma.||Includes Roxby Downs Granite.|Comagmatic with the Gawler Range Volcanics||
26613|Hiltaba Suite|64132|5|Briefly described|p1416 Fig.1, pp1432-1433.|Mesoproterozoic|Mesoproterozoic|Gawler Craton. Comagmatic with the Gawler Range Volcanics. Hosts the Olympic Dam deposit.|c.1590 - 1575 Ma.||Includes Balta Granite.||Granites, granodiorites, quartz monzonites, quartz syenite, quartz monzodiorites and mafic intrusions.|
26613|Hiltaba Suite|64133|4|Described|p1441-1450, p1457-1465      ||||~1575-1600 Ma (zircon U-Pb).||Includes Balta Granite.|Intrudes the Gawler Range Volcanics in places.|Comprises granites, granodiorites, quartz monzonites, quartz syenite and quartz monzodiorites. Contains both I-and-A-type compositions.|
26613|Hiltaba Suite|64135|5|Briefly described|p1499|Mesoproterozoic|Mesoproterozoic|Central and eastern Gawler Craton. Igneous intrusions with associated hydrothermal alteration, brecciation and IOGC mineralisation.|c.1600 - 1580 Ma (Ferris et al. 2002).||Includes Balta and Hiltaba Granites.|||26-SEP-14
26613|Hiltaba Suite|64313|5|Briefly described|p450 Fig. 1|Mesoproterozoic|Mesoproterozoic|Age: <1600Ma. Geological province: Gawler Craton. See also p451 Figs.2a,b.||||||09-FEB-10
26613|Hiltaba Suite|64319|6|Mentioned|p353, p355 Fig.1, p362-363|||Gawler craton. Its granites are uranium and thorium rich, generating unusually high heat flow.|||Includes Roxby Downs Granite.||Granites.|
26613|Hiltaba Suite|64576|6|Mentioned|p625, p625 Fig. 2|Mesoproterozoic|Mesoproterozoic|Age: 1595-1575Ma. ||||||
26613|Hiltaba Suite|64722|5|Briefly described|Fig. 2 p3-6, p14, 22, 27|Calymmian|Calymmian|Contains A-type felsic pluton. Geochemical data indicate a within-plate, possibly backarc, tectonic setting.|1600 - 1575 Ma.|||Coeval with, and genetically related to, the Gawler Range Volcanics.||11-APR-12
26613|Hiltaba Suite|64725|5|Briefly described|p58 Fig.2, p69.|Mesoproterozoic|Mesoproterozoic|Gawler Craton.|||Includes Roxby Downs Granite.||Granites.|
26613|Hiltaba Suite|64739|6|Mentioned|pp264-266, p278. |Mesoproterozoic|Mesoproterozoic|Gawler Craton. High temperature felsic intrusions.|1589-1578 Ma.|||||
26613|Hiltaba Suite|64740|6|Mentioned|p284 Fig.1, p285, pp293-294.|Mesoproterozoic|Mesoproterozoic|An enriched granite-rhyolite suite associated with postulated near margin continental back-arc setting at the northern margin of Archean Gawler Craton.|c.1595-1575 Ma.|||Intrudes St Peter Suite.||
26613|Hiltaba Suite|64741|6|Mentioned|p311|||||||||07-FEB-11
26613|Hiltaba Suite|64828|5|Briefly described|p1064 Fig. 1|Mesoproterozoic|Mesoproterozoic|Geological province: Gawler Craton.||||||04-MAR-09
26613|Hiltaba Suite|65219|6|Mentioned|p27 Fig.1|||||||||22-SEP-09
26613|Hiltaba Suite|65220|6|Mentioned|p19, p20|Calymmian|Calymmian|Age: 1595 - 1575 Ma. Previously regarded as anorogenic, due to mild extension, growing evidence now suggests compressional regime||||||10-DEC-09
26613|Hiltaba Suite|65221|5|Briefly described|p26, p32|Mesoproterozoic|Mesoproterozoic|Intrudes Wallaroo Group, Moonabie Formation and McGregor Volcanics||||||
26613|Hiltaba Suite|65375|5|Briefly described|p12, pp23-24.|Mesoproterozoic|Mesoproterozoic|Dominant unit in northern Yorke Peninsula basement.|1600-1580 Ma.|||||
26613|Hiltaba Suite|65376|4|Described|p10, pp147-153, pp215-217. |Mesoproterozoic|Mesoproterozoic|Most metallogenically significant magmatic unit in the Gawler Craton. Hosts IOCG and Au-only deposits in Olympic Domain. Includes A-type granitoids forming large batholiths and smaller plutons.|1596-1575 Ma.||Includes Charleston, Tickera, Calca, Roxby Downs, Balta and Arthurton Granites.|Co-magmatic with Gawler Range Volcanics.|Granites with 70 to 80% SiO2 dominate the Suite; locally includes hornblende-bearing quartz monzodiorite, quartz monzonite and granodiorite.|
26613|Hiltaba Suite|65385|5|Briefly described|pS128-pS129, pS131 Tab.2, pS132, pS135|Calymmian|Calymmian|Granite and adamellite. 1595-1575 Ma. Coeval with the Gawler Range Volcanics.||||||08-MAR-12
26613|Hiltaba Suite|65390|4|Described|p10, p18, p21, p22 Fig.3, p25-27|Calymmian|Calymmian|Intrudes Gawler Range Volcanics. Is overlain unconformably by Pandurra Formation. Mostly oxidised, K-feldspar dominant granite. Syn- to post- tectonic (Kararan Orogeny) setting, evidently associated with Fe-oxide-Cu-Au mineralisation in eastern Gawler Craton. Age of ~1595-1575 Ma from U-Pb zircon analysis (Younger Rb-Sr ages given are likely to be inaccurate). Highly variable geochemistry and Sm-Nd isotope analysis. Includes Wirrda and White Dam Subsuites; Balta, Buckleboo, Calca, Charleston, Minnipa, Roxby Downs, Tickera and Wudinna Granites.||||||
26613|Hiltaba Suite|65455|5|Briefly described|p9 Fig. 5|Mesoproterozoic|Mesoproterozoic|Voluminous suite in the Archean to Proterozoic Gawler Craton. Contains numerous examples of uraniferous igneous rocks.|||Includes Roxby Downs granite.|||09-MAY-12
26613|Hiltaba Suite|65483|5|Briefly described|p17,19,  22, 26, Fig. 1, 5|Calymmian|Calymmian|Gawler Craton. Age: 1595-1575 Ma. Bimodal magmatic suite depleted in Ba, Nb, Sr, P and Ti. Coeval with Gawler Range Volcanics.||||||04-MAR-13
26613|Hiltaba Suite|65485|6|Mentioned|Fig 1|Mesoproterozoic|Mesoproterozoic|||||||
26613|Hiltaba Suite|65772|6|Mentioned|p228, p229 Fig.2|Calymmian|Calymmian|1595-1575 Ma||||||
26613|Hiltaba Suite|65915|5|Briefly described|p3 Fig.2, p5, p18|Calymmian|Calymmian|Intrudes Wallaroo Group. ~1590-1575 Ma. Includes Charleston Granite.||||||
26613|Hiltaba Suite|65922|4|Described|p9-10, p17 Tb.2, p22-24, p29 Fig. 6|Calymmian|Calymmian|Massive, medium to coarse-grained granite and adamellite; minor aplite and pegmatite. Intrudes Gawler Range Volcanics. Hypabyssal emplacement synchronous with felsic magmatism of the Gawler Range Volcanics. U-Pb zircon age of 1581 +/- 16 Ma given. Geochemistry described. Synchronous with Hiltaba Suite intrusions.||||||
26613|Hiltaba Suite|66302|4|Described|p4-6, p34, p41-42, p44-p46, p55-56 |Calymmian|Statherian|Gawler Craton. A-type felsic magmatism. Ages derived from Flint et al, 1993 and Creaser and Cooper, 1993, respectively. See also p68-p72, p75, p77, p84, p92. |1600 +/- 16 Ma to 1575 +/- 6 Ma ||Includes the Lady Jane Diorite, Curramulka Gabbronorite and the Balta, Calca, Buckleboo, Ambrosia, Big Tank, Tickera, Arthurton, Roxby Downs, Kychering, Partridge, Munjeela and Pegler Granites.|Intrudes the Sleaford Complex.|Highly fractionated granite to granodiorite, ranging in composition from quartz-monzonite through to two-mica granite; minor mafic rocks also occur.|
26613|Hiltaba Suite|66519|6|Mentioned|pp31-33.|Early Mesoproterozoic|Early Mesoproterozoic|Gawler Craton. Associated with a major tectonic/tectonothermal episode; associated with major mineral systems including Cu-Au-U-rare earth elements and Au-only mineralisation.|c.1595-1575 Ma.|||||
26613|Hiltaba Suite|66522|6|Mentioned|p28.|Proterozoic|Proterozoic|Gawler Craton. Likely source of zircons of this age found in Kooringa Member.|c.1590 Ma.|||||
26613|Hiltaba Suite|66575|6|Mentioned|p948,|||Coeval with Gawler Range Volcanics. Felsic.||||||
26613|Hiltaba Suite|66916|5|Briefly described|p7, p9, p13, p16|Calymmian|Calymmian|Part of the Olympic IOCG Province. A high-temperature fluid flow related to magmatism of this unit is proposed to have formed the bulk of the skarn at Punt Hill Cu-Au-Zn-Pb deposit.|c.1590-1580 Ma.|||||
26613|Hiltaba Suite|67027|5|Briefly described|p348, p351 Table 1. |Mesoproterozoic|Mesoproterozoic||1589 +/- 16 Ma (U-Pb: Creaser & Cooper 1993).|||Intrudes Gawler Range Volcanics. Is overlain by Pandurra Formation.|Coarse-grained adamellite, granite.|
26613|Hiltaba Suite|67028|6|Mentioned|p362|||See also Hiltaba Suite Granitoids (p361-362, p367, p372-3).||||||24-APR-12
26613|Hiltaba Suite|67058|5|Briefly described|p480 Fig.4.|Proterozoic|Proterozoic||||||Granite, adamellite.|
26613|Hiltaba Suite|67112|6|Mentioned|p3 Fig.2|Mesoproterozoic|Mesoproterozoic|Gawler Craton.||||||
26613|Hiltaba Suite|67127|5|Briefly described|p104-105|||Enriched in REE, Y and fluorine. Whole rock geochemistry suggests that high fluorine concentration in the melt caused REE to behave incompatibly during magmatic crystallisation, thus producing an REE-rich late stage fluid.||||Coeval with the Gawler Range Volcanics.|Magmatic rocks.|
26613|Hiltaba Suite|67181|5|Briefly described|p616 Fig.1|Mesoproterozoic|Mesoproterozoic|Gawler Craton. References: Fairclough et al. 2003, Payne et al. 2003.|1590-1575 Ma|||||
26613|Hiltaba Suite|67462|5|Briefly described|Map legend.|||||||||
26613|Hiltaba Suite|67536|5|Briefly described|Map Legend|Calymmian|Statherian|Gawler Craton. Informally subdivided into two parts. Inheritance (Tickera) ca. 1750 Ma.|1613 +/- 19 Ma - 1575 +/- 7 Ma||Includes Curramulka Gabbronorite.||Mafic to felsic plugs; granite to adamellite, lesser quartz monzodiorite. Quartz monzonite and granodiorite.|
26613|Hiltaba Suite|67540|6|Mentioned|p25|Mesoproterozoic|Mesoproterozoic|Gawler Craton. Magmatism contemporaneous with Gawler Range Volcanics.||||||
26613|Hiltaba Suite|67581|6|Mentioned|p44 Fig.8, p45|||Gawler Craton.|1600-1575 Ma.|||||
26613|Hiltaba Suite|67870|6|Mentioned|p16|||High heat-producing granites from this unit, although not imaged seismically, may be the cause of high heat flows recorded along seismic line 09TE-01, potentially attractive for geothermal energy exploration.||||||
26613|Hiltaba Suite|67900|5|Briefly described|p20, 22, 32|Mesoproterozoic|Mesoproterozoic|Widespread across central and southern Gawler Craton. Many plutons show no deformation at all.|||Charleston Granite.||A bimodal intrusive Suite; dominantly granites. Considerable geochemical variation; mostly fractionated; silica generally >70%.|
26613|Hiltaba Suite|67909|5|Briefly described|p124-127, 130, 135-136, 139-141|Mesoproterozoic|Mesoproterozoic|Gawler Silicic-dominated Large Igneous Province. After the first mention, it appears in text as Hiltaba Suite.|1598 +/- 2 Ma to 1583 +/- 7 Ma.|||Co-magmatic with, and locally intrudes, Gawler Range Volcanics.|Typically medium-grained, locally porphyritic, pink granite as large batholiths, smaller granite intrusions; minor quartz monzodiorite and quartz monzonite.|
26613|Hiltaba Suite|67980|5|Briefly described|p548 Fig.1b, p566|Calymmian|Calymmian|Intrusive equivalent of Gawler Range Volcanics.|c.1590-1570 Ma (Daly et al., 1998).|||||
26613|Hiltaba Suite|68128|5|Briefly described|p2, p53|Mesoproterozoic|Mesoproterozoic|Gawler Craton.|c. 1595-1575 Ma||||Granite and adamellite.|
26613|Hiltaba Suite|68131|5|Briefly described|p2 Fig.1, p52-54, p68, p71-72, p77, p87|Mesoproterozoic|Mesoproterozoic|See also p92-93. Mapped with Bimbowrie and Moolawatana Suites as a single unit. A megacrystic granite was dated at 1598 +/- 7 Ma.|c.1590-1580 Ma.||Calca Granite.||Granitic rocks and felsic porphyry.|
26613|Hiltaba Suite|68158|5|Briefly described|p4-5||||1595-1575 Ma.|||Intrudes Moonabie Formation and Corunna Conglomerate. Is overlain by Backy Point Formation.|Granite with porphyritic and granophyric phases; pink granite and granodiorite, common large pink K-feldspar phenocrysts, minor fine- to very coarse-grained phases.|
26613|Hiltaba Suite|68208|6|Mentioned|p31 Fig.1||||c.1595 - 1575 Ma|||||
26613|Hiltaba Suite|68715|6|Mentioned|p28, p32 Fig.6|||Radiogenic granitic rocks; potential source areas for U.|||||Granitoids.|07-APR-17
26613|Hiltaba Suite|69004|4|Described|p16, p18, p24|Mesoproterozoic|Palaeoproterozoic|Gawler Craton. Co-magmatic with the Gawler Range Volcanics. The source of widespread Cu-Au-U mineralisation across the Gawler Craton.|||||Felsic granite plutons with distinctive pink hue due to hematite dusting of feldspar crystals.|
26613|Hiltaba Suite|69019|6|Mentioned|p30 Fig.10.|Calymmian|Calymmian|Gawler Craton. See also reference to Hiltaba Granite (p29 Fig.9).|c.1590 Ma.|||||
26613|Hiltaba Suite|69023|6|Mentioned|p27 Fig.8|||Gawler Craton.||||||
26613|Hiltaba Suite|69048|6|Mentioned|p3|||Eyre Peninsula / Yorke Peninsula.||||||
26613|Hiltaba Suite|69203|6|Mentioned|p59||||c.1590 Ma.|||||
26613|Hiltaba Suite|69255|5|Briefly described|p788|Calymmian|Statherian|Part of a large, mainly felsic, magmatic system which included also the Gawler Range Volcanics. Associated with IOCG mineralisation.|c.1600-1585 Ma.|||||
26613|Hiltaba Suite|69554|6|Mentioned|p128|Mesoproterozoic|Mesoproterozoic|Central Gawler Craton. Part of a voluminous felsic large igneous province.|c.1590 Ma.|||||
26613|Hiltaba Suite|69648|6|Mentioned|p34|||||||||
26613|Hiltaba Suite|69649|5|Briefly described|p26-28, p6 Fig.4, p7, p8 Fig.6, p9-10|Mesoproterozoic|Mesoproterozoic|See also p34, p36, p41-42, p47, p48-50, p54-55. Large plutons concentrated around N and E margins of the Nuyts Domain. An integral part of the deformation/tectonic history of the W Gawler Craton. In the Kondoolka Batholith, contains rafts of basement metasedimentary enclaves. Various ages given. Several outcrops W of Childara Outstation have been reassigned to Tunkillia Suite.|1595-1575 Ma.||||Generally massive granites, granodiorites; variable textures.|26-FEB-15
26613|Hiltaba Suite|69650|6|Mentioned|p1|||Gawler Craton.||||||04-FEB-16
26613|Hiltaba Suite|69654|6|Mentioned|p1, 23, 25|||Gawler Craton.||||||
26613|Hiltaba Suite|69666|6|Mentioned|p27 Fig.3|Mesoproterozoic|Mesoproterozoic|||||||
26613|Hiltaba Suite|69748|5|Briefly described|p179-181, 183, 188|Mesoproterozoic|Mesoproterozoic|Moonta-Wallaroo region, Olympic IOGC Province.|1600-1575 Ma.||Tickera, Arthurton Granites; Curramulka Gabbronorite.||Granites, mafric-ultramafic intrusive rocks.|
26613|Hiltaba Suite|70025|6|Mentioned|p22|Mesoproterozoic|Mesoproterozoic|Geological province: Mawson Craton.||||||
26613|Hiltaba Suite|70027|5|Briefly described|p56,58|Calymmian|Calymmian|Geological province: Gawler Craton. Emplaced into Gawler Craton ca. 1600-1570 Ma post-Kimban Orogeny.|ca. 1600-1570 Ma|||Coeval with Gawler Range Volcanics.||17-JUL-19
26613|Hiltaba Suite|70286|6|Mentioned|p883-886, 891-892|Mesoproterozoic|Mesoproterozoic|Eastern Gawler Craton.|1600-1570 Ma.||||Bimodal but dominantly felsic A-type magmatism.|
26613|Hiltaba Suite|70333|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Probably includes five seperately mapped  facies, one of which is named Cultana Subsuite. Another age is given: 1578 +/- 7 Ma (Tarcoola/Kingoonya).|1581 +/- 16 Ma (Hiltaba).||Probably includes Cultana Subsuite.||Granite/adamellite [?!!], anomalous metals in veins. Separately-mapped: quartz-feldspar porphyry; alkali-feldspar granite; feldspar-phyric granophyric monzogranite; alkali-feldspar microgranite; micro-syenogranite.|11-JAN-16
26613|Hiltaba Suite|70334|4|Described|p2-3,12-14,17,75, p84|Statherian|Statherian|Geological province: Gawler Craton. Bimodal intrusive suite; widely distributed and found outcropping around GRV outcrops in cental and southern Gawler Craton. Lithologically and geochemically variable (megacrystic varieties to fine-grained subvolcanic varieties) (Stewart and Foden, 2003), Mostly fractionated, enriched in HFSE elements (U,Th and K), and with SiO2 contents generally >70% (Flint, 1993), indicative of a heterogeneous source (Hand et al., 2007). Suggested tectonic setting is a far-field continental back-arc setting accompanied locally by regional-scale high-temperature metamorphism and compressional deformation (Hand et al., 2007, Wade et al., 2012). Hosts several mineralisation styles, including IOCG-U, Pb-Zn skarn or epithermal mineralisation.|~1590-1575 Ma||Includes Cultana Subsuite.|Intrudes Gawler Range Volcanics.|High-T, fractionated granite to granodiorite.|14-OCT-19
26613|Hiltaba Suite|70337|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Another age is given: 1581 +/- 16 Ma (Hiltaba).|1578 +/- 7 Ma (Tarcoola/Kingoonya).||||Granite/adamellite, anomalous metals in veins.|
26613|Hiltaba Suite|70382|5|Briefly described|p27, p33-34, p35|Calymmian|Calymmian|Geological province: Yorke Peninsula. Associated with Gawler Range Volcanics.|~1590 Ma|||Intrudes the Wallaroo Group.|Granites and gabbros.|
26613|Hiltaba Suite|70405|6|Mentioned|p12 figure 4|Mesoproterozoic|Mesoproterozoic||1580 Ma|||||
26613|Hiltaba Suite|70511|6|Mentioned|p86-87, 96, 98|Mesoproterozoic|Mesoproterozoic|Central and eastern Gawler Craton. A constituent of the Gawler Silicic Large Igneous Province.|1595-1575 Ma (Hand et al., 2007).||Roxby Downs Granite.||Granites.|
26613|Hiltaba Suite|70657|6|Mentioned|p48|||Gawler Craton. Temporal relationship with the Ninnerie Supersuite (Curnamona Province).|||||I-A type.|
26613|Hiltaba Suite|70659|4|Described|p2-4, p6, p9-10, p48-49|Mesoproterozoic|Mesoproterozoic||1590-1575 Ma||Includes Tickera Granite, Roxby Downs Granite.|Intrudes Wallaroo Group, Moonabie Formation.|High-T fractionated granites, coarse grained porphyritic phase of large potassium feldspar phenocrysts in a groundmass of medium to coarse grained plagioclase, K-feldspar, quartz and biotite. Margins are dominated by pegmatite, silexite and aplite.|
26613|Hiltaba Suite|70721|6|Mentioned|p63-p64|Mesoproterozoic|Mesoproterozoic|Intrudes the Spencer Domain of the Gawler Craton.||||||
26613|Hiltaba Suite|70738|5|Briefly described|p185-186, 189, 196|Mesoproterozoic|Mesoproterozoic|Gawler Craton.|c.1595-1575 Ma.||Roxby Downs Granite.|Cogenetic with Gawler Range Volcanics.|Granite, granodiorite, quartz syenite and quartz monzodiorite plutons.|
26613|Hiltaba Suite|70789|5|Briefly described|p316, p318 Fig.2, p320-321|Mesoproterozoic|Mesoproterozoic|Gawler Craton basement. AFT results tabulated; central ages from 277 +/- 33 Ma to 409 +/- 64 Ma.|c.1595-1575 Ma.||||Variably uraniferous and fluorite-rich granites.|
26613|Hiltaba Suite|70816|5|Briefly described|p3-4|Calymmian|Calymmian|Geological province: Gawler Ranges. Associated with Gawler Range Volcanics.|1590-1575 Ma||||High-T[emp] fractionated granites and minor mafic rocks|
26613|Hiltaba Suite|70893|5|Briefly described|p1-p4, p8|Calymmian|Calymmian|SHRIMP age derived from this volume are magmatic crystallisation age on monzogranite sample form Slade Point. Associated with widespread alteration and mineralisation in the Gawler Cration. A-type geochemical signatures. Petrography discussed in detail.|1585 +/- 7 Ma (SHRIMP)||||Massive to weakly foliated granite with enclaves of more biotite-rich granite.|05-SEP-19
26613|Hiltaba Suite|70947|5|Briefly described|p959-960|Calymmian|Calymmian|Geological province: Gawler Craton. |ca. 1590 Ma||Includes Roxby Downs Granite.|||
26613|Hiltaba Suite|70948|6|Mentioned|p974|Mesoproterozoic|Mesoproterozoic|Geological province: Gawler Craton.||||||
26613|Hiltaba Suite|71037|5|Briefly described|p20-21, p21 Fig.1, p24|Mesoproterozoic|Mesoproterozoic|Formation age shown as c. 1595-1575 Ma.|c. 1595-1575 Ma.|||Shown as older than Pandurra Formation. Co-magmatic with Gawler Range Volcanics.||
26613|Hiltaba Suite|71043|5|Briefly described|p103-104, p107|Calymmian|Calymmian|Flint et al. (1993). The major syn-mineralisation intrusive magmatic suite of the Gawler Craton. Extends from Olympic Dam to the western Gawler Craton.|c.1595-1575 Ma.|||||
26613|Hiltaba Suite|71129|5|Briefly described|p2,14,17-18,47,182|Calymmian|Calymmian|Geological Province: Gawler Craton. Widespread, high-T fractionated granites and minor mafic rocks over the Gawler Craton, associated with the Gawler Range Volcanics and Munjeela Suite. |1590-1575 Ma|||||
26613|Hiltaba Suite|71169|5|Briefly described|p78|Calymmian|Calymmian|Gawler Craton. Emplaced during the Hiltaba Event.|1595-1575 Ma||||A-type granitic rocks.|
26613|Hiltaba Suite|71235|6|Mentioned|p1, p5, p9||||c. 1590 Ma||Includes the Charleston Granite.|||
26613|Hiltaba Suite|71236|5|Briefly described|iv, p1-p2, p22-p23|Mesoproterozoic|Mesoproterozoic|Gawler Craton. Temporally and genetically associated with numerous IOCG deposits and prospects, including Olympic Dam, Prominent Hill, Oak Dam, Acropolis, Wirrda Well, Moonta-Wallaroo and Carrapateena.|c. 1595-1575 Ma||Includes the Cultana Subsuite.||Bimodal magmatic rocks.|
26613|Hiltaba Suite|71317|4|Described|p1-p2, p14-p16, p19-p20|Early Mesoproterozoic|Early Mesoproterozoic|Gawler Craton. Characterised by high magnetic intensity. See also p97, p112-p114, p117, p123-p125, p131-p137, p146, p153, p158-p159, p162-p166, p169, p172, p176.|c. 1595-1575 Ma||||Pale pink to reddish-brown, highly siliceous, alkali feldspar-rich, leucocratic biotite granites and minor mafic rocks.|
26613|Hiltaba Suite|71318|6|Mentioned|p28|||Geological province: Gawler Craton.||||||
26613|Hiltaba Suite|71322|5|Briefly described|p3, p91, p99-100, p103, p125, p135-136|Mesoproterozoic|Mesoproterozoic|This c.1595-1570 Ma magmatic event produced significant alteration in the central-northern Eyre peninsula and the eastern Gawler Craton. One undeformed granite at the Weednana Deposit was dated.|1584 +/- 5 Ma.||||Pink granite.|13-DEC-21
26613|Hiltaba Suite|71341|6|Mentioned|p179 fig 1|Mesoproterozoic|Mesoproterozoic||ca. 1580 Ma|||||
26613|Hiltaba Suite|71348|6|Mentioned|p200-201|Mesoproterozoic|Mesoproterozoic|Geological province: Gawler Craton. Associated with mineralisation including IOCG deposits of the eastern Gawler Craton.||||||01-JUL-19
26613|Hiltaba Suite|71413|5|Briefly described|p31-32, 37, 39|||Geological province: Gawler Craton. Lies on the boundary between Spence and Olympic domains (Roopena Fault Zone) of the southern Gawler Craton. Potentially endowed with uranium.|||Includes Samphire granite.|||31-MAY-19
26613|Hiltaba Suite|71418|5|Briefly described|p21,25|Mesoproterozoic|Mesoproterozoic|Geological province: Gawler Craton. Emplacement broadly corresponds to 1586+\-8 Ma age of alunite crystallisation and acid sulfate alteration of the Hutchison Group.||||||
26613|Hiltaba Suite|71534|5|Briefly described|p294-296, 301-302|Calymmian|Calymmian|Geological province: Gawler Craton. Ferroan, A-type felsic compositions with a subordinate mafic component and variable Sm-Nd and Lu-Hf isotopic composition reflecting crustal contamination of a mafic source by a heterogeneous crustal column (Allen et al., 2008; Belousova et al., 2009; Flint et al., 1993; Wade et al., 2012). Associated with renewed mantle input post-Kimban Orogeny. More evolved Hf isotope data show significant crustal melting.|c. 1595-1575 Ma|||||
26613|Hiltaba Suite|71536|4|Described|p1-p3, p11, p15, p22, p28|Calymmian|Calymmian|See also p119, p137, p148, p175, p181, p187. Additional ages of 1584 +/- 6 Ma and 1572 +/- 6 Ma are provided. Ages are SHRIMP U-Pb dates and are interpreted as the age of magmatic crystallisation. Petrography, zircon characteristics and geochronology results are discussed for two granite samples of this suite.|1584 +/- 4 and 1586 +/- 6 Ma||Includes the Charleston Granite.||Coarse-grained granites.|
26613|Hiltaba Suite|71559|5|Briefly described|p14, p15 Fig 1, p16 Fig 2, p19-24, p26|Calymmian|Calymmian|Geological province: Gawler Craton. Intrudes Paleoproterozoic basement. Crystallisation age via SHRIMP U-pb dating. Thermal drive for hydrothermal fluid within Progress-Eurilla fault.|1590-1575 Ma.||||Granite to granodiorite; coarse-grained K-feldspar megacrystic to fine-grained porphyritic or equigranular high level intrusives.|
26613|Hiltaba Suite|71560|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic||c.1590-1575 Ma (U-Pb).||||Granite to granodiorite; coarse-grained K-feldspar megacrystic to fine-grained porphyritic or equigranular high-level intrusives.|
26613|Hiltaba Suite|71618|6|Mentioned|p135|Calymmian|Calymmian|Geological province: Gawler Craton. Possible, but unlikely source of ~1500-1800 Ma detrital zircons in the Madura Formation, Loongana Formation and Decoration Sandstone.|c. 1590 Ma|||||
26613|Hiltaba Suite|71712|6|Mentioned|p409, p410 Fig 1, p411, p419|Calymmian|Calymmian|Also referred to as Hiltaba Suite granitoids (p411) and Hiltaba Suite intrusions (p419). Hosts mineralisation at Olympic Dam.|1595-1575 Ma|||Coeval with Gawler Range Volcanics.||31-MAR-20
26613|Hiltaba Suite|71859|5|Briefly described|p3-p6|Mesoproterozoic|Mesoproterozoic|Southern Gawler Craton. Comagmatic with the Gawler Range Volcanics.|c. 1590-1575 Ma|||||
26613|Hiltaba Suite|71862|5|Briefly described|p3-p4, p8-p9, p12, p21|Calymmian|Calymmian|Central Gawler Craton. Co-magmatic with the St Peter Suite.|c. 1595-1575 Ma||||Felsic and minor mafic intrusive rocks.|
26613|Hiltaba Suite|71895|5|Briefly described|p2, p10, p126, p141, p147|Mesoproterozoic|Mesoproterozoic|Punt Hill region. Average magnetic susceptibility and gravity values provided.|c. 1590 Ma|||||
26613|Hiltaba Suite|72058|5|Briefly described|p172, p186, p190, p192|||Eyre Peninsula, Gawler Craton. Metasomatism in this suite is comparable to that found in the Middleback Ranges Granitoids.|1600 Ma|||Equivalent to the Charleston Granite.||16-MAR-21
26613|Hiltaba Suite|72065|4|Described|p103-106,111-112,115,117-118,120|Calymmian|Calymmian|Geological province: Gawler Craton. Abbreviated as HS in text. Comagmatic with Gawler Range Volcanics; together known as the Mesoproterozoic Gawler LIP. Emplacement age at 1597+\-7 Ma to 1375.7+\-4.3 Ma. Comprise a series of white to pink, medium- to coarse grained, equigranular intrusive rocks that range from pristine to strongly altered and deformed (Flint, 1993). Of limited surface outcrop. Crystal clusters: 'HS-type' fine- to medium-grained magnetite-apatite+\-titanite+\-biotite-chlorite+\-zircon. Evolution of parental magma chamber after initial crystal formation within the magma chamber and formation of GRV lavas, increasing melt water content stabilises biotite and other accessory minerals to form HS-type lavas.|||Includes Roxby Downs Granite, Tickera Granite, Kychering Granite.||Predominantly granitic, but also include monzodiorite, quartz monzonite, granodiorite, gabbro and norite.|
26613|Hiltaba Suite|72089|6|Mentioned|p2|Mesoproterozoic|Mesoproterozoic|Gawler Craton. ||||||
26613|Hiltaba Suite|72090|4|Described|p1-p2, p9-p10, p11, p13, p17|Calymmian|Calymmian|Gawler Craton. Intrusive equivalents of the Gawler Range Volcanics. Coeval with mineralisation in the Gawler Craton. See also p58-p59, p73-p74, p78, p91, p100, p107, p112, p115, p117, p120.|c. 1595-1570 Ma||||A- and I-type felsic intrusives and mafic intrusives; fine to very coarse-grained pink to light red granite.|
26613|Hiltaba Suite|72237|4|Described|p28|Mesoproterozoic|Mesoproterozoic|Geological province: Gawler Craton.|1595-1575 Ma|||||
26613|Hiltaba Suite|72242|6|Mentioned|p27|Calymmian|Calymmian|Geological province: Coompana Province, Western Gawler Craton. Associated with Kararan Orogeny. Coeval with Birksgate Complex and Toolgana Supersuite, and extensive oceanic crust formation.||||||
26613|Hiltaba Suite|72454|5|Briefly described|p1-2, p20, p49, p53-54|Mesoproterozoic|Mesoproterozoic|Dates are indistinguisable from those of Gawler Range Volcanics. Part of the Gawler Craton.|||||Includes granite.|
26613|Hiltaba Suite|72459|5|Briefly described|p5-6, p8, p10, p14|Mesoproterozoic|Mesoproterozoic|Gawler Craton. Plutons widespread across the central Gawler Craton. Associated with known mineralisation such as Cu-Au-U-REE and Pb-Zn mineralisation.|~1600 Ma|||||
26613|Hiltaba Suite|72461|6|Mentioned|p6|||||||||
26613|Hiltaba Suite|72462|5|Briefly described|p1-3, p5, p7|Calymmian|Calymmian|Gawler Craton. A-type felsic rocks. Occurs as widely distributed plutons. Part of a silicic large igneous province; originally contiguous with the Benagerie Volcanic Suite and Ninnerie Supersuite. Interpreted to have a heterogeneous source region derived from a depleted mantle sources with a significant crustal component. Features IOCG and gold mineralisation type mineral associations.|ca 1590-1575 Ma||||Dominated by granite to granodiorite; typically megacrystic, but sometimes fine-grained and porphyritic; contains minor mafic phases.|
26613|Hiltaba Suite|72463|6|Mentioned|p2|Mesoproterozoic|Mesoproterozoic|||||||
26613|Hiltaba Suite|72464|5|Briefly described|p1-2, 24, 27-28|Mesoproterozoic|Mesoproterozoic|Gawler Craton.|||||Granites.|
26613|Hiltaba Suite|72488|5|Briefly described|p1, 4-6, 14, 16-18|||Eastern Gawler Craton. Voluminous, bi-modal intrusives. Hosts IOCG deposits (eg Olympic Dam). Likely emplaced in a post-subduction switch from compressional to extensional setting. The parent magmas are the major source of metals throughout the Olympic Cu-Au Province. Appears as Hiltaba Intrusive Suite in Fig.1.|~1594 Ma.|||Intrudes Mulgathing Metamorphic Complex, Donington Suite and Wallaroo Group. Co-magmatic with Gawler Range Volcanics.|Granites.|
26613|Hiltaba Suite|72725|6|Mentioned|p41, p43-44|Calymmian|Statherian||1600-1575 Ma||||Granite, syenite, quartz monzonite, granodiorite, monzodiorite: coarse, megacrystic to equigranular, to fine-grained, granophyric, equigranular or porphyritic. Undeformed to locally strongly deformed. Minor mafic to ultramafic intrusive rocks.|
26613|Hiltaba Suite|72934|6|Mentioned|p9, p12|Calymmian|Calymmian|Northern Gawler Craton. Similar in age and isotopic character to the rocks of the Coompana Province.|1590-1575 Ma|||||
26613|Hiltaba Suite|72949|6|Mentioned|p32-34, p36-42|Calymmian|Calymmian|Mafic rocks of the suite have eNd(1590 Ma) = -5 to 0 (Wade et al., 2019). Part of the Gawler Siliceous Large Igneous Province. Changed from A-type to I-type granite compositions after c. 1.59 Ga.|ca. 1.595-1.575 Ga||||Includes F-rich mafic melts|
26613|Hiltaba Suite|73026|5|Briefly described|p4 fig1.2, p6, p9-11|Mesoproterozoic|Mesoproterozoic|Central/western Eyre Peninsula.|c.1595-1570 Ma||Includes the Curamulka Gabbronorite.|Underlies the Gawler Range Volcanics.|Granite and gabbroic intrusives.|
26613|Hiltaba Suite|73027|5|Briefly described|p4, p6, p9-11|Mesoproterozoic|Mesoproterozoic|Central/western Eyre Peninsula, central and southern Gawler Craton. Implicated as the source of heat (and metals?) for the IOCG mineral systems of the eastern Gawler Craton. Contains greenschist facies fabrics on the Yorke peninsula.|c. 1600-1575 Ma||Includes the Curamulka Gabbronorite.||Granite and gabbroic intrusives.|
26613|Hiltaba Suite|73030|6|Mentioned|p2147-2150, p2152|Calymmian|Calymmian|Gawler Craton. Subdivided into two broad subsuites: less oxidized Kokatha type and more oxidized Roxby Downs type [also called the Roxby Downs sub-suite]. The Kokatha-type granites are associated with gold-dominant mineralization in the central Gawler gold province and those of the Roxby Downs type are broadly spatially associated with the Olympic Cu-Au province in the eastern Gawler Craton. Constitutes the intrusive equivalent of the Gawler Range Volcanics. Voluminous felsic magmatism resulted from both fractional crystallization and widespread crustal melting.|ca. 1595 to 1570 Ma|||Equivalent to Gawler Range Volcanics and Munjeela Suite.||
26613|Hiltaba Suite|73092|6|Mentioned|p1-3, p50, p54-55, p59|Calymmian|Statherian|Yorke Peninsula region. Ages are of magmatic crystallisation. Dated samples are altered granite from drillholes KD10 (187.8-189 m) and KD4 (250.25-251.6 m). [An older magmatic crystallisation age of 1737 +/- 28 Ma was obtained from a granite sampled from CUR D5 drillhole (78.5-78.9 m); see Table 1. This sample appears to have been attributed to a different unit later in the report without explanation; see Moonta Porphyry Member].|c. 1580 Ma, 1556 +/- 25 Ma, 1546 +/- 19 Ma||Tickera Ganite||May include medium- to coarse-grained, pink/red-coloured, biotite/magnetite-bearing granite.|
26613|Hiltaba Suite|73099|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Gawler Craton.|||||Interpreted granite intrusives.|
26613|Hiltaba Suite|73103|5|Briefly described|Map legend.|||Is shown in the Solid Geology Interpretation map, below the main Whyalla 250k map.||||||
26613|Hiltaba Suite|73104|6|Mentioned|p2-4, p72|Mesoproterozoic|Mesoproterozoic|Intrudes pre-Mesoproterozoic basement rocks in the Mount Double area.|||||Includes granite and porphyritic felsic intrusions.|
26613|Hiltaba Suite|73110|5|Briefly described|Map legend.|||Shown in the Solid Geology Interpretation map below the main PORT AUGUSTA map.||||||
26613|Hiltaba Suite|73130|6|Mentioned|[poster]|Calymmian|Calymmian||c. 1595-1575 Ma|||||
26613|Hiltaba Suite|73155|5|Briefly described|p263-265, p274-275, p277-279, p282-287|Calymmian|Calymmian|Gawler Craton. Granites and mafic plutons are in the southern and western zones of the Mount Woods Domain, granites are less abundant in central zone. High to moderate gravity response; mafic plutons have highly stippled magnetic texture; granite plutons have generally low Bouguer gravity response, highly magnetic stippled texture. Emplaced at shallow levels and entrained in upper plate of Mount Woods Metamorphic Core Complex. Ages from southern Mount Woods Domain: 1587+/-4 Ma, 1586+/-3 Ma (Jagodzinski, 2005).|ca. 1595-1575 Ma||Balta Granite, Balta Granite Suite||Includes granites and mafic plutons.|
26613|Hiltaba Suite|73162|6|Mentioned|p448, p449, p451|Mesoproterozoic|Mesoproterozoic|Gawler Craton. Associated with volcanism of Gawler Silicic Large Igneous Province. Co-magmatic with Gawler Range Volcanics.|1595-1575 Ma||||Granites and minor mafic rocks.|
26613|Hiltaba Suite|73165|5|Briefly described|p619-623, 634-638|Calymmian|Calymmian|Widely distributed across the Gawler Craton. Bimodal magmatism during a period of regional deformation. Vary across the A-, I- and S-type range. Characteristic chemical signatures of high Th, low CaO, MnO and Sr concentrations, evolved Sm-Nd isotope signatures depending on region.  Differences in chemistry of the Hiltaba Suite granites between domains. Hiltaba Suite Granites and Hiltaba Granite Suite used in Fig 1, p620.|ca 1595-1575 Ma||Tickera Granite, Arthurton Granite, Curramulka Gabbronorite||Granites. Bimodal magmatism with mafic and felsic components.|
26613|Hiltaba Suite|73166|6|Mentioned|p644, 645, 656|Mesoproterozoic|Mesoproterozoic|Gawler Silicic Large Igneous Province, Gawler Craton. Contemporaneous with Gawler Range Volcanics. Previously described as syenite (Paterson, 1986). 1.59 Ga age shown in Fig. 1, p645.|ca 1.6 Ga, 1.59 Ga|||Intrudes Gawler Range Volcanics.|Granite. Minor host rock in the Acropolis prospect.|
26613|Hiltaba Suite|73227|6|Mentioned|p24|Calymmian|Calymmian||> 1575 Ma|||||
26613|Hiltaba Suite|73230|6|Mentioned|p8, p11-12|Mesoproterozoic|Mesoproterozoic|May be related to gold-bearing quartz veins in the Harris Greenstone Domain.||||||
26613|Hiltaba Suite|73233|5|Briefly described|p26, p27 Fig.1, p28-31|Mesoproterozoic|Mesoproterozoic|Gawler Craton, Nyuts Domain and eastern Fowler Domain. Deformed and metamorphosed in eastern Fowler Domain, relatively low magnetic intensity.|1586+/-9 Ma, 1568+/-11 Ma|||Intrudes St Peter Suite|Igneous Intrusions. Includes foliated granites.|
26613|Hiltaba Suite|73234|6|Mentioned|p4-5, p19|||Associated with the Gawler Range Volcanics and contemporaneous with Fresh Well Formation.|||||Intrusive rocks.|
26613|Hiltaba Suite|73235|6|Mentioned|p52-53, p57, p63|Calymmian|Calymmian|Gawler Craton. Gawler Range Volcanic region. Intrusion resulted in a strong regional overprint. Intrusion of magma, although widespread across the Gawler Craton, was commonly focused on major regional structures. Hosts gold mineralisation in the Western Gawler, Wudinna, ?Tunkillia, and Olympic mineral fields of the Kararan (Hiltaba Suite) gold mineral system.|1590-1575 Ma||||Includes mafic and ultramafic rocks.|
26613|Hiltaba Suite|73252|6|Mentioned|p4|||Gawler Craton.||||||
26613|Hiltaba Suite|73256|4|Described|p557-576|Calymmian|Calymmian|Gawler Craton. Subduction zone setting. Regional compression, locally interpreted as extensional and compressional environment of emplacement. Spatially and temporally associated with IOCG and Au [other] mineralisation. Varies across the A-, I- and S-type range, is highly fractionated, and is enriched in HFSE, U, Th, and K. Unique geochemical features in different parts of the craton. Geochemical composition of zircon may be useful for distinguishing this unit from the coeval Gawler Range Volcanics. [See article for petrographic descriptions, whole-rock geochemistry, and zircon morphological and compositional characterisation].|ca 1595-1575 Ma||Roxby Down Granite|Coeval with Gawler Range Volcanics.||
26613|Hiltaba Suite|73263|6|Mentioned|p591-592|Calymmian|Calymmian|Gawler Craton. Extensive throughout the craton. Contemporaneous with high-sulfidation epithermal silver and porphyry copper-gold mineralisation.|ca 1598-1575 Ma|||Equivalent to Gawler Range Volcanics.||
26613|Hiltaba Suite|73298|6|Mentioned|p1072 Fig.1, p1078 Fig.6|Calymmian|Calymmian|Gawler Craton.|ca 1590 Ma|||||
26613|Hiltaba Suite|73302|6|Mentioned|p32-33, 50, 54|Mesoproterozoic|Mesoproterozoic|With the Gawler Range Volcanics, represents a large igneous province.|c.1595-1575 Ma.|||||02-MAR-23
26613|Hiltaba Suite|73429|6|Mentioned|p105, p114|Calymmian|Calymmian|Gawler Craton.|c. 1590-1580 Ma|||||
26613|Hiltaba Suite|73493|5|Briefly described|p711-712, p714 Fig.1, p716 Fig.3, p727|Calymmian|Calymmian|Gawler Craton. See also p725 Fig.12, p726 Fig.13, p728.|ca 1595-1575 Ma||Curramulka Gabbronorite|||
26613|Hiltaba Suite|73524|6|Mentioned|p4|||Gawler Craton. Correlative of Ninnerie Suite.||||||
26613|Hiltaba Suite|73644|5|Briefly described|p1, p3, p12-13, p15-16|Mesoproterozoic|Mesoproterozoic|Generally accompanied by metasomatism on the Yorke Peninsula, assumed to be cogenetic with Hiltaba Suite intrusives and termed the Oorlano Metasomatite.|1595-1575 Ma||Curramulka Gabbronorite, Oorlano Metasomatite|Intrudes Wallaroo Group|Granitic and gabbroic rocks.|
26613|Hiltaba Suite|74361|5|Briefly described|p163-164, 169, 171, 173, 175-177|Mesoproterozoic|Mesoproterozoic|Reeve et al. (1990). Gawler Craton. One of the major sources of the ""bedded clastic facies"" in the Olympic Dam Breccia Complex.",,|~1590 Ma.||Roxby Downs Granite.|Co-magmatic with Gawler Range Volcanics. Locally intrudes Gawler Range Volcanics.|Predominantly granitic batholiths and plutons; considerable compositional variation including minor mafic plutons.|
30605|Hiltaba Supersuite|23248|6|Mentioned|p169||Mesoproterozoic|||||||
30605|Hiltaba Supersuite|24197|6|Mentioned|p72|||Geological Province: Gawler Craton.||||||07-FEB-11
30605|Hiltaba Supersuite|24256|6|Mentioned|p48|||||||||
30605|Hiltaba Supersuite|24567|5|Briefly described|p160 Tb. 2|Mesoproterozoic|Mesoproterozoic|Age: ca1580Ma. Geological Province: East Gawler Craton.||||||09-MAY-05
30605|Hiltaba Supersuite|50537|6|Mentioned|p1.1, 3.1|||I-Type.||||||
30605|Hiltaba Supersuite|50605|5|Briefly described|p(ii), 1.3, 8.1, Table 1.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Gawler Craton & Curnamona Province. Age: 1592-1590Ma.||||||
30605|Hiltaba Supersuite|66529|6|Mentioned|p30|||Has strong similarities with Esmeralda Supersuite (Qld), discussed in connection with potential for uranium field.||||||
30605|Hiltaba Supersuite|69091|6|Mentioned|p206|||||||||
30605|Hiltaba Supersuite|69591|6|Mentioned|p83|||Associated with iron oxide-copper-gold mineralisation. Mentioned as having similarities to the Esmeralda Supersuite in QLD.||||||
75706|Hodgkinson Granodiorite|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Mount Painter area.|1552 +/- 4 Ma.|||||
75706|Hodgkinson Granodiorite|67430|6|Mentioned|p38|||Hore and Neumann (in prep.). Informally referred to as the Paralana Granodiorite. Mount Gee - Mount Painter area, Mount Painter Inlier.|1550 Ma (Fraser and Neumann, 2010).||||I-type. Consists of plagioclase, quartz, biotite, minor K-feldspar and amphibole.|
75706|Hodgkinson Granodiorite|69562|5|Briefly described|p670 Tb.5||||1552 +/- 4 Ma (Neumann, 2001).||||Medium-grained granodiorite.|
75706|Hodgkinson Granodiorite|70384|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|SHRIMP U-Pb zircon ages. Metamorphic zircon rims dated at ~520 Ma and ~460 Ma.|1552+/-4Ma, 1563+/-3Ma SHRIMP.||||Granodiorite, medium-grained, equigranular, with biotite, weak fabric.|17-JAN-19
75706|Hodgkinson Granodiorite|73061|6|Mentioned|p1076 Fig.6|Mesoproterozoic|Mesoproterozoic|Mount Painter Province.||||||
26307|Hogan Dolomite|22772|5|Briefly described|Table13.1|Cryogenian|Cryogenian|||||||
26307|Hogan Dolomite|22857|5|Briefly described|Tb. 13.1 (insert p70-71)|Willouran|Willouran|Of the Curdimurka Subgroup (Callanna Group).||||||
26307|Hogan Dolomite|24175|3|Fully described|p9|Neoproterozoic|Neoproterozoic|Of Curdimurka Subgroup. Overlies Recovery Formation; underlies Cooranna Formation.  Max. thickness: 645m.||||||13-FEB-08
26307|Hogan Dolomite|24321|5|Briefly described|Map legend|Adelaidean|Adelaidean|Parent: Curdimurka Subgroup||||||
26307|Hogan Dolomite|37854|2|Defined|p11|Adelaidean|Adelaidean|Prob.Late Willouran||||||
26307|Hogan Dolomite|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Willouran||||||
26307|Hogan Dolomite|40294|6|Mentioned|p9|||||||||
26307|Hogan Dolomite|41402|6|Mentioned|p42|||||||||
26307|Hogan Dolomite|41403|4|Described|p65|||||||||
26307|Hogan Dolomite|42222|5|Briefly described|p12|||||||||
26307|Hogan Dolomite|43052|5|Briefly described|p175,Table 6.1|||Of Curdimurka Subgroup.||||||13-FEB-08
26307|Hogan Dolomite|60718|5|Briefly described|p49 Fig. 2|Adelaidean|Adelaidean|Geological Province: Adelaide Geosyncline.||Of Curdimurka Subgroup (Callanna Group).||Unconformably overlies Recovery Formation.||15-APR-11
26307|Hogan Dolomite|64796|6|Mentioned|p190 Fig.8, p194 Tb.2, p200 Fig.10, p202|Neoproterozoic|Neoproterozoic|Willouran Ranges. Appears in Fig.8 without the lithology.||Unit in Curdimurka Subgroup.||Overlies Recovery Formation. Is overlain by Cooranna Formation.||
26307|Hogan Dolomite|72492|3|Fully described|p2 Fig.1, p3, p4 Fig.3d, p5 Fig.4b|Neoproterozoic|Neoproterozoic|In Willouran Ranges. See also p7 Tb.1, p10 Tb.2, p11 Tb.3.||Curdimurka Subgroup||Overlies Recovery Formation and underlies Cooranna Formation.|Includes stromatolites, halite casts and desiccation cracks.|16-SEP-20
26307|Hogan Dolomite|73222|6|Mentioned|p7|Tonian|Tonian|Willouran Ranges. Torrensian.||Curdimurka Subgroup, Callanna Group, Warrina Supergroup||Underlain by Recovery Formation. Overlain by Cooranna Formation. Equivalent to Arkaba Hill Beds.||
26617|Holowilena Ironstone|22510|5|Briefly described|p38,41|||Of the Yudnamutana Subgroup.  Age: Sturtian||||||13-OCT-04
26617|Holowilena Ironstone|22631|6|Mentioned|p177|||||||||
26617|Holowilena Ironstone|22851|6|Mentioned|14|||Geol province Adelaide Geosyncline||||||
26617|Holowilena Ironstone|22854|6|Mentioned|P10|||||||||
26617|Holowilena Ironstone|23250|5|Briefly described|p1124 Fig.2||Cryogenian|of Umberatana Group. Correlate of Areyonga Formation.||||||
26617|Holowilena Ironstone|23818|5|Briefly described|p64 Fig.22, p65|Neoproterozoic|Neoproterozoic|Of the Yudnamutana Sub-Group. Overlying unit: Wilyerpa Quartzite.||||||
26617|Holowilena Ironstone|23913|4|Described|p110 Fig. 2|Adelaidean|Adelaidean|Geological Province: Central Flinders Zone.  Of the Umberatana Group.  Overlying Unit: Wilyerpa Formation.||||||
26617|Holowilena Ironstone|29780|6|Mentioned|p32|||||||||
26617|Holowilena Ironstone|30178|6|Mentioned|p19|||||||||
26617|Holowilena Ironstone|30801|6|Mentioned|p5|||Sturtian. Table P5-6||||||
26617|Holowilena Ironstone|30802|4|Described|p8|||Sturtian. See also P12||||||
26617|Holowilena Ironstone|30807|6|Mentioned|p103|||Suggested map symbol||||||
26617|Holowilena Ironstone|32146|6|Mentioned|Fig.3|||||||||
26617|Holowilena Ironstone|32510|6|Mentioned|Table 1|||||||||
26617|Holowilena Ironstone|32724|6|Mentioned|Fig.1|||Correlation||||||
26617|Holowilena Ironstone|33794|6|Mentioned|p28|||||||||
26617|Holowilena Ironstone|34269|6|Mentioned|Table 1|||||||||
26617|Holowilena Ironstone|34535|6|Mentioned|p65|||Sedimentary||||||
26617|Holowilena Ironstone|35255|6|Mentioned|p13|||||||||
26617|Holowilena Ironstone|35904|6|Mentioned|p9|||||||||
26617|Holowilena Ironstone|37238|6|Mentioned|p367|||||||||
26617|Holowilena Ironstone|37932|6|Mentioned|p537|||||||||
26617|Holowilena Ironstone|38157|6|Mentioned|Table IV|||||||||
26617|Holowilena Ironstone|39344|6|Mentioned|Map legend|Precambrian|Precambrian|Sturtian||||||
26617|Holowilena Ironstone|39348|6|Mentioned|Map legend|Precambrian|Precambrian|Sturtian||||||
26617|Holowilena Ironstone|40225|4|Described|Map sheet|||||||||
26617|Holowilena Ironstone|40294|3|Fully described|p41|||See also P15||||||
26617|Holowilena Ironstone|41405|3|Fully described|p137|||||||||
26617|Holowilena Ironstone|42222|6|Mentioned|p15|||||||||
26617|Holowilena Ironstone|42643|6|Mentioned|p21|||Adelaide geosyncline||||||
26617|Holowilena Ironstone|42813|6|Mentioned|p18|||||||||
26617|Holowilena Ironstone|43052|5|Briefly described|p183,Table 6.1|||||||||
26617|Holowilena Ironstone|43845|5|Briefly described|Fig3 p43, 42||Neoproterozoic|In Umberatana Group||||||12-JUL-16
26617|Holowilena Ironstone|44659|5|Briefly described|map legend|||Marinoan, lithology.||||||
26617|Holowilena Ironstone|45155|6|Mentioned|p44|||||||||
26617|Holowilena Ironstone|46865|6|Mentioned|p49|||||||||
26617|Holowilena Ironstone|60959|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Of the Yudnamutana Subgroup. Dark red, thinly laminated iron rich siltstone; medium to coarse grained gritty sandstone and glacially derived pebbly siltstone.||||||
26617|Holowilena Ironstone|62085|6|Mentioned|p20 fig 5|Cryogenian|Cryogenian|||Umberatana Group||Overlies Pualco Formation. Is overlain by Wilyerpa Formation.||
26617|Holowilena Ironstone|62724|5|Briefly described|p16, p17 Fig. 4|||In the Flinders Ranges. Ferruginous ironstone originally containing finely-divided hematite, metamorphosed to crystalline magnetite. Overlain by Wilyerpa Formation. Geological Province: Olary DomainCurnamona Province.||||||07-FEB-11
26617|Holowilena Ironstone|64797|5|Briefly described|p158, p166 Tb.7, p173|||Adelaide Rift Complex. S-isotope data.||||||
26617|Holowilena Ironstone|64801|6|Mentioned|p112|Neoproterozoic|Neoproterozoic|||||||
26617|Holowilena Ironstone|65892|5|Briefly described|p33 Fig.18. |Cryogenian|Cryogenian|||Unit in Umberatana Group.||Overlies Pualco Formation. Is overlain by Wilyerpa Formation.||
26617|Holowilena Ironstone|65925|5|Briefly described|Appendix 2.||||||||Hematitic siltstone, purplish red, thinly bedded; red shale; grey siltstone, minor dolomite, medium-grained quartzite, ironstone lenses.|
26617|Holowilena Ironstone|68276|6|Mentioned|p69|||Flinders Ranges. Associated with the Sturtian glaciation. The ""Ironstone"" is omitted.",,||||Conformably overlies Pualco Tillite. Is overlain disconformably by Wilyerpa Formation.|Haematite-jaspilite and associated ferruginous argillite, with sporadic lenses of boulders (some grooved and striated), ferruginous diamictite including sorted argillite, and rare lenses of haematite-jaspilite with rafted dropstones.|
26617|Holowilena Ironstone|70031|5|Briefly described|p245|Cryogenian|Cryogenian|Adelaide Geosyncline. Associated with Sturtian glaciation.||Unit of Yudnamutana Subgroup.||Overlain by Warcowie Dolomite Member. Laterally equivalent to Benda Siltstone and Pualco Tillite.||
26617|Holowilena Ironstone|70082|6|Mentioned|p2|Cryogenian|Cryogenian|Flinders Ranges. Contains red beds.||||||
26617|Holowilena Ironstone|70323|3|Fully described|p211-222|Cryogenian|Cryogenian|Central Flinders Ranges, Adelaide Geosyncline. Associated with Sturtian glaciation. Not laterally extensive in the Yudnamutana Subgroup. Subdivisible into 3 facies: 1) ferruginous shale and siltstone facies (deep marine, turbiditic); 2) ferruginous diamictite facies (reworking of unconsolidated sediment, muddy debris flow from synsedimentary tectonism) and 3) laminated hematite and jasper facies (syndepositional, diagenetic). Unlike typical Archean-Paleoproterozoic iron formations, it typifies Neoproterozoic iron formations in lacking iron-silicates and iron-carbonates. Hematite is intepreted as early diagenetic replacement of precursor iron oxyhydroxides produced by reaction of ferrous (Fe2+) iron dissolved in ferruginous Sturtian oceans with molecular oxygen (O2) (Lepp and Goldich, 1964; Ewers, 1983; Beukes and Klein, 1992). Jasper is interpreted to be from co-precipitation of silica adsorbed onto the iron oxyhydroxides (Slack et al., 2007; Fischer and Knoll, 2009).|c. 660 Ma|Unit of Yudnamutana Subgroup.||Overlain unconformably to conformably by Wilyerpa Formation. Passes gradationally into Pualco Tillite.|1) Red-purple shales and siltstones, fine-grained hematite laths, microcrystalline quartz, clay minerals 2) similar to ferruginous shale and siltstone facies but greater proportion of lithic clasts, detrital zircons 3) laminated hematite and jasper.|
26617|Holowilena Ironstone|70407|5|Briefly described|p103 Fig 2, p113|Neoproterozoic|Neoproterozoic|Age: Sturtian.||Of Umberatana Group.||||
26617|Holowilena Ironstone|71237|14|Not recorded|p10, 17|||||||||
26617|Holowilena Ironstone|72449|5|Briefly described|p1, p2 Map Legend|Neoproterozoic|Neoproterozoic|Shown as part of diapir formation diagram, p1.|700 Ma.|||Overlies Pualco Tillite and underlies Wilyerpa Formation.|Dark red, thinly laminated iron-rich siltstone; includes medium to coarse-grained gritty sandstone and glacial pebbly siltstone.|
26617|Holowilena Ironstone|72473|6|Mentioned|p4-5|||Probably deposited towards the end of the first Sturtian glaciation. Exposed between the Oraparinna and Enorama Diapirs in the central Flinders zone.||||Overlain by Wilyerpa Formation.||
75889|Honeymoon Granite|67540|2|Defined|p25, pp26-28, p36 Tb.3, p39 Fig.2|Calymmian|Calymmian|New name; after Honeymoon Mine, 39 km NNW of Mingary. Type locality: drillhole YAM052C, between 162-200m. Definition reference: this article and Fricke and Hore (2011). Mulyungarie Domain, Curnamona Province. Airborne magnetics and EM data show that the Honeymoon Granite intrudes the Bimba Formation. ~1580 Ma. Concordia intercept age, SHRIMP II.|1541 +/- 59 Ma (Jagodzinski and Fricke 2010).|Of the Ninnerie Supersuite.||Intrudes the Bimba Formation.|Quartz-plagioclase-alkali feldspar-muscovite-biotite granite. Non magnetic. S-type.|05-FEB-16
75889|Honeymoon Granite|67900|6|Mentioned|p19|||||||||
75889|Honeymoon Granite|68126|5|Briefly described|p1, p4, p7-14, p41, p46-47|||Mulyungarie Domain, Curnamona Province. Known from geophysical imagery and a drill-hole intersection. Very low magnetic susceptibility values. Believed to be the source of U in the Honeymoon uranium deposit. Age determination problems associated with high-U are discussed. Geochemical analyses detailed.|1541 +/- 59 Ma (Concordia intercept age).|Ninnerie Supersuite.|||Variably-altered, quartz-plagioclase-alkali feldspar-muscovite-biotite granite. Abundant quartz-feldspar veining and brittle fracturing.|
75889|Honeymoon Granite|69562|5|Briefly described|p669-673, p674 Fig.6, p676|||S Lake Frome region. Contains up to 40 ppm U; spatially associated with Honeymoon and East Kalkaroo uranium deposits. Shows intensive potassic alteration.|1541 +/- 59 Ma (Jagodzinski & Fricke, 2010).|Unit in Ninnerie Supersuite.|||Quartz-plagioclase-alkali feldspar-muscovite-biotite granite.|
75889|Honeymoon Granite|69650|2|Defined|p4 Tb.1, p2, p6, p13, p16, p22, p29|Calymmian|Calymmian|See also p37-39, p41, p45. New name, after Honeymoon Mine, 39 km NNW of Mingary. Mulyungarie Domain, Curnamona Province. Type section described from drillcore. Drillhole YAM052C, GDA 94, 470325 mE, 6485715 mN (Fig. 14), within the interval 162?200 m.. Subsurface: appears on TMI images as several discrete non-magnetic circular to lobate shapes disrupting regional fold structures, and often surrounded by informally named Mundaerno Granite, Bimbowrie Suite. Concordia intercept age; also an age of ~1580 Ma (SHRIMP U-Pb zircon) is interpreted from high-U magmatic zircons. Geochemistry outlined.|1541 +/- 59 Ma; Jagodzinski and Fricke, 2010.|Unit in Ninnerie Supersuite.||Intrudes Bimba Formation.|Quartz-plagioclase-alkali feldspar-muscovite-biotite granite; non-magnetic. S-type.|25-NOV-22
75889|Honeymoon Granite|70658|5|Briefly described|p33-34, 36-37|Mesoproterozoic|Mesoproterozoic|Curnamona Province. Geochemistry briefly described. Buried granitic bodies S of the Honeymoon Mine.|~1580 Ma.||||Quartz-plagioclase-alkali feldspar-muscovite-biotite granite. Non-magnetic. S-type.|
75889|Honeymoon Granite|73251|6|Mentioned|p36|Calymmian|Calymmian|[Written as Honeymoon-type granite]. Curnamona Province. Includes uraniferous crystalline rock.|c. 1590 Ma|Ninnerie Supersuite||||
29818|Hopeful Hill Basalt|24472|5|Briefly described|p5 Tb.1|Archean|Archean|Geological Province: Harris Greenstone Domain, Gawler Craton. Age: >2460 Ma. Parent: Mulgathing Complex.||||||07-NOV-08
29818|Hopeful Hill Basalt|43052|4|Described|p42, Table 3.2|||Of Mulgathing Complex||||||
29818|Hopeful Hill Basalt|50605|5|Briefly described|8.7|||Of the Mulgathering Complex. Geological Province: Gawler Craton & Curnamona Province.||||||
29818|Hopeful Hill Basalt|65376|5|Briefly described|p190, p196-197.||||c.2458 +/- 10 Ma.|Unit in Mulgathing Complex.||Intruded by Glenloth Granite veins.|Metabasalt, medium- to fine-grained with plagioclase, hornblende and diopside; weak to strongly developed vertical foliation; epidote and calcite veins common. Local pillow basalt.|
29818|Hopeful Hill Basalt|66302|6|Mentioned|p12|||||Mulgathing Complex|||Basalt.|
29818|Hopeful Hill Basalt|68128|6|Mentioned|p2|Palaeoproterozoic|Archaean|Gawler Craton.||Mulgathing Complex||||
29818|Hopeful Hill Basalt|73230|4|Described|p6, p8, p12|Siderian|Neoarchean|Gawler Craton. Domain: Harris Greenstone. Has locally anomalous Ni-Cu and Ni-PGE and is predominantly low in sulfer based on limited testing. Interlayered with Kenella Gneiss. Shows pillow structures, characteristic of subaqueous deposition. Thought to be genetically related to Lake Harris Komatiite via fractional crystallisation; thus, was [probably] emplaced at c. 2510 Ma. May be an extrusive equivalent of South Lake Gabbro but further work is needed.|Older than c. 2458 Ma (magmatic)|Mulgathing Complex||Intruded [crosscut] by Glenloth Granite.|Medium- to fine-grained metatholeiitic basalt with plagioclase, hornblende and diopside.|
29818|Hopeful Hill Basalt|73235|6|Mentioned|p56, p61|||Hosts gold mineralisation in the Harris Greenstone mineral field of the Sleafordian gold mineral system and in the Labyrinth mineral field of the Kararan (Gawler Range Volcanics) gold mineral system.||||||
81592|Horn Ridge Granite|72065|6|Mentioned|p112|||Geological province: Olympic Province, Gawler Craton. Contains 'HS-type' crystal clusters: fine- to medium-grained magnetite-apatite+\-titanite+\-biotite-chlorite+\-zircon. (HS: Hiltaba Suite type).||||||
75471|Hot Springs Gneiss|63866|6|Mentioned|p43|||||||||
75471|Hot Springs Gneiss|66302|6|Mentioned|p49|Calymmian|Calymmian|Ages derived from McLaren et al. (2006) and Neumann et al. (2009).|1585 to 1575 Ma |||||
75471|Hot Springs Gneiss|69562|5|Briefly described|p669, p670 Tb.5, p673 Fig.5|||Mount Painter Inlier. Contains 7 to 427 ppm U: excellent source of leachable U. Has intensive metasomatic overprints.|1582 +/- 6 Ma (Fraser and Neumann, 2010).||||Coarse-grained augen granitic gneiss with strong biotite foliation.|
78896|Hutchison Supergroup|73026|5|Briefly described|p9|Paleoproterozoic|Paleoproterozoic||||Includes the Cleve Group and the Darke Peak Group.|||
78896|Hutchison Supergroup|73027|5|Briefly described|p9,|Palaeoproterozoic|Palaeoproterozoic||c. 1750 Ma||Includes the Cleve Group and the lower Darke Peak Group.|||
78896|Hutchison Supergroup|73122|5|Briefly described|p17, p18 Fig.1, p19-20, p21 Fig.4, p22|Palaeoproterozoic|Palaeoproterozoic|SE Gawler Craton. Age is given as Mesoproterozoic on p17. See also p25 Fig.6, p30, 32, 34-35, 40-43.|||Warrow Quartzite.|Is intruded by Moody Suite.|Quartzites and garnet-sillimanite metasedimentary rocks.|
78896|Hutchison Supergroup|73634|6|Mentioned|p2 Fig.1, p4|Paleoproterozoic|Paleoproterozoic|Eyre Peninsula, Gawler Craton.|||||Metasedimentary rocks.|
79868|Idandanoo Member|64801|5|Briefly described|p111-112, p116, p119|Cryogenian|Cryogenian|New, informal name. Unconformity-bound genetic increment of strata [?]. Sediments derived from nearby exposed diapirs. In part equivalent to, or replacing the Wundowie Member of the Enorama Shale?||Enorama Shale.|||Shallow-water stromatolitic, ooid, intraclast and lithoclast limestones, overlain by deeper-water green siltstones which shallow up to stromatolitic limestone again.|21-JUN-17
79868|Idandanoo Member|72473|6|Mentioned|p4|||||||||
39945|Ifould Granite|24472|5|Briefly described|p5 Tb.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Harris Greenstone Domain, Gawler Craton. Age: ~1680 Ma.||||||07-NOV-08
27045|Ilkina Formation|22613|4|Described|p25|||||||||
27045|Ilkina Formation|22614|5|Briefly described|map|Pleistocene|Pliocene|||||||
27045|Ilkina Formation|41619|6|Mentioned|Map Legend|late Pliocene||||||||
27045|Ilkina Formation|42466|5|Briefly described|Map Legend|||||||||
27045|Ilkina Formation|42475|5|Briefly described|p23|||||||||
27045|Ilkina Formation|44133|5|Briefly described|p186, 180 Fig. 10.22|Early Pleistocene|Late Pliocene|Geological Province: Eucla Basin. Thickness: 5m. ||||||
27045|Ilkina Formation|44695|5|Briefly described|Map Legend|Pleistocene|Pliocene|||||||
27045|Ilkina Formation|61155|5|Briefly described|p17|Holocene|Late Pliocene|Age: <2Ma. Geological Province: Eucla Basin.||||||
27045|Ilkina Formation|64646|6|Mentioned|p23 Fig. 3, p24 Fig. 4|Pliocene|Pliocene|Geological Province: Gawler Craton.||||||08-FEB-10
27045|Ilkina Formation|65922|5|Briefly described|p25 Tb. 4, p26, p43|Pleistocene|Late Pliocene|Laminated white and yellowish sand and sandy to gritty clay; bands of gypsum and selenite. Lacustrine.||||||
27045|Ilkina Formation|67462|5|Briefly described|Map legend.|Pliocene|Pliocene|Eucla Basin.||||||
27045|Ilkina Formation|68715|6|Mentioned|p30 Fig.5|Pliocene|Pliocene|Bunda Plateau and SW Gawler Craton, Eucla Basin. Late Pliocene age.||||||
27045|Ilkina Formation|69598|6|Mentioned|p9|Late Pliocene|Late Pliocene|||||Overlies the Narlaby Formation.||
27045|Ilkina Formation|69648|4|Described|p28-29, map legend|Pleistocene|Pliocene|Thin, lacustrine and fluvial sequence of muds, sands and interlaminated gypsum horizons. Occurs in some playa lakes along SW margin of Ooldea Range. Outcrops poorly forming low benches (<0.5 m high) above lake floor. Thickness: typically <2.5 m. Best exposure along Ifould Lake margins on BARTON that locally include distinctive, chara oogonia-rich, cross-bedded, calcareous, sandstone facies and very thin beds of carbonate mudstone, locally reworked (Benbow et al. 1995b, Rankin et al. 1996) and thin outwash deposits including silcrete and ferricrete. Age: older than aeolian sands of Great Victorian Desert.||||Overlies Garford Formation; similar to Milyera Formation (Lake Eyre Basin).|Lithologically distinctive with common, laminated character and occcurrence of blue and grey clays; sorting generally good; laminae and laminated cap of gypsum in upper part.|
27045|Ilkina Formation|69649|5|Briefly described|p32|||Deposited in the Narlaby Paleochannel; crops out along SW margin of Gawler Ranges and forms lake floors (eg Lake Bring). Marks change to arid climate in late Cenozoic.|||||Laminated clay, silt and sand.|
27045|Ilkina Formation|73108|5|Briefly described|Map legend.|Pleistocene|Eocene||||||Clay, silt, sand, laminated to thinly bedded, local clasts of silcrete and ferricrete. Locally capped by gypsum crust. Palaeochannel fill.|
23661|Immarna Group|22613|6|Mentioned|p18|||||||||
23661|Immarna Group|24112|5|Briefly described|p270|Pliocene|Pliocene|Geological Province: Officer Basin||||||
23661|Immarna Group|42816|6|Mentioned|p18, p22|||||||||
23661|Immarna Group|42959|5|Briefly described|p58 Fig.3|||||||||
23661|Immarna Group|43026|5|Briefly described|Table 1,p586|||||||||
23661|Immarna Group|43052|5|Briefly described|Table 2.1|||||||||
23661|Immarna Group|44133|5|Briefly described|p178|Tertiary|Tertiary|Geological Province: Eucla Basin. ||||||
23661|Immarna Group|69648|4|Described|p4, p21|||Of Benbow (1990, 1994) and Benbow et al. (1995a and 1995b). Eucla Basin. Inner platform margin of basin is dominated by terrestrial clastic sediments, deposited in river and coastal environments. |||Burdunga Subgroup, Yarle Sandstone, Garford Formation||Predominantly terrigenous clastic sediments deposited in shallow marine, coastal and nonmarine environments.|
23661|Immarna Group|71317|4|Described|p137, p143|Pliocene|Miocene|Intersected in all three MDSP drillholes. Ranges from 39.45 to 49.35m thick. Fluvial to lacustrine deposits.||||Overlies the Pondanna Dacite Member.|Moderately to highly weathered conglomerate with minor mudstone and highly weathered, light grey, moderately to well sorted, fine to very coarse-grained, clay-rich pebbly sandstone and conglomerate with subangular to subrounded rhyolite clasts.|
23661|Immarna Group|71559|5|Briefly described|p19|Pleistocene|Eocene|Geological province: Gawler Craton.|||||Conglomerate and sandstones, moderately to highly weathered, pale-yellowish orange to reddish orange, poorly to moderately sorted. Fine- to coarse-grained, with sub-angular and sub-rounded volcanic clasts. Clay and mudstone, grey to orange, massive.|
23661|Immarna Group|71560|5|Briefly described|Map legend.|Pleistocene|Eocene|Subsurface only. Fluvial to lacustrine deposits.|||Garford Formation.||Conglomerates and sandstones, moderately to highly weathered, pale yellowish-orange to reddish-orange, poorly to moderately sorted; fine- to coarse-grained, with sub-angular to sub-rounded volcanic clasts. Clay and mudstone, grey to orange, massive.|
23661|Immarna Group|72090|5|Briefly described|p47, p50, p55, p57|||Gawler Craton.|||||Light grey, very fine- to very coarse-grained, moderately to well sorted, sub-angular to sub-rounded, clast rhyolite, highly weathered conglomerate.|
23661|Immarna Group|73099|5|Briefly described|Map legend.|Pliocene|Eocene|Meramangye and Tallaringa Palaeochannels.|||Garford Formation; Burdunga Subgroup.|Overlies Neales River Group.||
34749|Ingomar Quartzite Member|22889|5|Briefly described|p39|Adelaidean|Adelaidean|See p39 for location of type section and details of new stratigraphic unit. The Ingomar Quartzite Member superseds the former Ingomar Quartzite as the unit has been down graded from formation to member status, see p33 for details of change.||||||
33817|Innamincka Formation|13497|5|Briefly described|p55, p105, p114|Ordovician|Ordovician|Warburton Basin.||||Unconformably overlain by the Arrabury Formation.|Redbeds and quartzites.|
33817|Innamincka Formation|22527|6|Mentioned|p 5|||||||||
33817|Innamincka Formation|23154|5|Briefly described|Map Legend|Cambrian|Cambrian|Geological Province - Warburton Basin.||||||
33817|Innamincka Formation|23155|5|Briefly described|p9|Ordovician|Ordovician|The Innamincka Formation has not been drilled on STRZELECKI, but may occur on the down faulted western flank of the Gidgealpa Ridge.||||||
33817|Innamincka Formation|23287|6|Mentioned|p105|||Two distinct acritarch fossil assemblages found within.||||||12-NOV-15
33817|Innamincka Formation|44133|5|Briefly described|p4 Fig. 7.2, 31, 33|Late Ordovician|Late Cambrian|Geological Province: Eastern Warburton Basin.||||||
33817|Innamincka Formation|62537|6|Mentioned|p191 Fig.2. |Middle Ordovician|Early Ordovician|Warburton Basin.||||||
33817|Innamincka Formation|63056|5|Briefly described|p80, p81 Fig. 2|Early Cambrian|Early Cambrian|Thickness: 1700m. Geological Province: Warburton Basin. Extensive deltaic interbedded siltstone and rippled glauconitic sandstone; acritarchs, bryozoa, conodonts.||||||06-FEB-07
33817|Innamincka Formation|63224|6|Mentioned|p9|||Geological Province: Warburton Basin.||||||07-FEB-08
33817|Innamincka Formation|63978|5|Briefly described|p5||Late Ordovician|Overlies the Kalladeina Formation. Red bed sequence. Passes laterally into the Dullingari Group. Geological province: Warburton Basin.||||||07-FEB-11
33817|Innamincka Formation|65489|5|Briefly described|p14, p32 Fig.11, p96, p118-120|Middle Ordovician|Early Ordovician|Eastern Warburton Basin. Thick redbed succession. Appears as Innamincha Formation on p96.|||Includes Mudrangie Sandstone.|Overlies Kalladeina Formation.|Extensive deltaic interbedded siltstone and rippled glauconitic sandstone.|
33817|Innamincka Formation|67402|4|Described|p260, p261|Chewtonian|Lancefieldian|Warburton Basin. Deposited in a prograding shoreline or delta environment. ||||Overlies the Kalladeina Formation. Overlain by the Dullingari Group. Grades laterally into the Pando Formation and the Dullingari Group.|Quartzose sandstone, siltstone and glauconitic sandstones.|
33817|Innamincka Formation|67536|6|Mentioned|Map Legend|||Warburton Basin.|||||Deltaic red-bed shale, siltstone and sandstone|
33817|Innamincka Formation|68731|5|Briefly described|p115, p168, p170 Fig 3.83, p171, p207|Late Ordovician|Early Ordovician|~ 1700 m thick. Warburton Basin. Deltaic depositional environment.  Upper age is not defined but is probably Middle or early Late Ordovician.|||Includes the Mudrangie Sandstone.|Unconformably overlain by the Callamurra Member.|Includes extensive deltaic interbedded siltstone and rippled glauconitic sandstone; acritarchs, bryozoa, conodonts.|
33817|Innamincka Formation|69023|6|Mentioned|p78, p80|||Warburton Shelf. Shallow marine to paralic environments of deposition.||||||
33817|Innamincka Formation|69449|5|Briefly described|p34:2 Fig.34.2; 34:4|Ordovician|Ordovician|Warburton Basin.||||Overlies Dullingari Group. Is overlain by Mudrangie Sandstone. Probable correlative of Pacoota or Stairway Sandstones.|Interbedded shale and sandstone red beds.|12-JUL-16
33817|Innamincka Formation|69673|6|Mentioned|p149, p149 fig 120|||||||||
33817|Innamincka Formation|69982|1|Redefined|p31, p33-40, p10, p13, p17-19, p45|Early Ordovician|Early Ordovician|See also p160, p220, p223-224, Appendix 1. Formerly "Innamincka Red Beds" (Sprigg, 1967), an informal name for a thick redbed suite extensively cored in Innamincka 1. Replaced by Innamincka Formation which was [erroneously] thought to interfinger with the top part of Kalladeina Formation (Gravestock, 1995), and which is [re]defined in this study. Section in the type well Innamincka 1 is from 2149.1 to 2280.21 m. Warburton Basin. Over 1700 m thick. Subdivided into two members, one of which is named. Six lithofacies are described. Brief thin section descriptions. Composite log shown. Bedding dip angles in wells listed. Details of wells with hydrocarbon shows.|||Includes Mudrangie Sandstone Member.|Is in (thrust) fault contact with Kalladeina Formation.|Lower thick redbed member of mainly bioturbated red mudstone and shale, cross-laminated siltstone and minor intraclastic pebbly sandstone; under horizontal to cross-laminated, moderately well-sorted quartzose sandstone.|12-NOV-15
33817|Innamincka Formation|70749|5|Briefly described|p43-45, p54-55|Ordovician|Ordovician|Warburton Basin. Extends into undercover Thomson Orogen. Shallow marine deposits adjacent to carbonate shelf.||||Overlies Kalladeina Formation.|Lower red calcareous sandstone occasionally with glauconite and heavy mineral laminae, overlain by interbedded fossiliferous mudstone, siltstone and sandstone with bioturbation.|
33817|Innamincka Formation|71283|6|Mentioned|p472 Fig.2|Ordovician|Ordovician|||||||
33817|Innamincka Formation|71342|6|Mentioned|Ch10 p20|Ordovician|Ordovician|Warburton Basin.||||||
33817|Innamincka Formation|71965|6|Mentioned|p894|||Geological province: Thomson Orogen.||||||
33817|Innamincka Formation|73244|6|Mentioned|p86|Silurian|Ordovician|Warburton Basin. Deposited in a deltaic/prograding shoreline environment.||||||
33817|Innamincka Formation|73479|5|Briefly described|p156 Fig.2, p157|Silurian|Ordovician|Warburton Basin. Deltaic/prograding shoreline depositional environment. Regional erosion of upper part represents unconformably boundary to the overlying Cooper Basin.|ca 485-435 Ma|||Overlies Pando Formation, Narcoonowie Formation||
38132|Investigator Granite Gneiss|60707|2|Defined|p619 Aoo. 1|Paleoproterozoic|Paleoproterozoic|Fine- to medium-grained mid-pink to pale grey, weakly  to moderately foliated K-feldspar-bearing quartz-plagioclase gneiss.  Age: 1762+/-11Ma (U-Pb zircon ICP-MS).  Geological Province: Gawler Craton (Nuyts Domain).  See also p611, p613-614.||||||11-MAR-17
38132|Investigator Granite Gneiss|63224|6|Mentioned|p10|||Geological Province: Gawler Craton.||||||07-FEB-08
38132|Investigator Granite Gneiss|63866|5|Briefly described|p5, p9, p18, p31|Statherian|Statherian|Nuyts Domain. Age is an LA-ICPMS U-Pb zircon age. Intrudes Mesoproterozoic granites within the Nuyts Domain. Appears as Investigator granite-gneiss on p9 and p31.|1762 +/- 11 Ma (Cooper and Belousova, 2004)|||||
38132|Investigator Granite Gneiss|66302|6|Mentioned|p23, p25|Statherian|Statherian|Nuyts Domain, Gawler Craton. |1762 +/- 11 Ma (Cooper and Belousova, 2004)|||||
38132|Investigator Granite Gneiss|67536|5|Briefly described|Map Legend|Statherian|Statherian|Gawler Craton.|1762 +/- 11 Ma||||Granitic gneiss to porphyritic granite.|
38132|Investigator Granite Gneiss|68131|5|Briefly described|p72|||Seal Point, SE Flinders Island.|1762 +/- 11 Ma.||||Granite gneiss.|
81106|Iron Baron granite|72058|5|Briefly described|p184, 178, 192|Mesoarchean||Middleback Ranges, Gawler Craton. Informal name. Zircon morphology and analysis is described. see also Iron Baron S. p181, 182. 183, 185, 186, 190, sample MB153. Age is by U-Pb SHRIMP dating. Reported age is from most concordant data point. Results display significant discordance. Pb loss likely.|3089 +/- 9 Ma (Min crystallisation age)||||Altered granite.|16-MAR-21
82215|Iron Magnet granite|72058|5|Briefly described|p177, 176, 183, p185-186|Mesoarchean|Mesoarchean|Samples MB84, MB85 - both leucogranite and appear to be Iron Baron samples in Table 1, but described as Iron Magnet samples p176, p181, p182, p185-186 . Major and trace element geochemistry discussed.  U-Pb SHRIMP dated.,  MB83 - sheared granite - not dated. See also p171, 173, 174.|3023+/-33 Ma ign. cryst.|||||16-MAR-21
81107|Iron Monarch granite|72058|5|Briefly described|p184, 185, 186, 192|Mesoarchean||Middleback Ranges, Gawler Craton. Informal name. Zircon morphology and analysis is described. Sample MB157. See also p174, 181, 182, 183. Age is by U-Pb SHRIMP dating. Reported age is from most concordant data point. Results display significant discordance.|3165 +/- 8 Ma (min. cryst)||||leucogranite.|16-MAR-21
83701|Jacaranda Ridge Sandstone|73594|5|Briefly described|p45, p50-51|||Otway Basin. Informal subdivision of the upper Sawpit Shale introduced by Camac and Boult (2008). Appears to be restricted to the Penola Trough.||Upper Sawpit Shale|||Thin, laterally extensive unit interpreted as a sheet sand.|
34732|Jarrold Basalt Member|22889|2|Defined|p33 & p37|Adelaidean|Adelaidean|Type section location advised p37.  This Member correlates with the Uraidla Phylite of the Aldgate Sandstone.||||||
30532|Jena Basalt|62537|6|Mentioned|p191 Fig.2. |Middle Cambrian|Middle Cambrian|Warburton Basin.||||Intrudes Dullingari group.||
30532|Jena Basalt|63056|5|Briefly described|p81 Fig. 2|Middle Cambrian|Middle Cambrian|Basalt and agglomerate. Geological Province: Warburton Basin.||||||01-APR-14
30532|Jena Basalt|65489|5|Briefly described|p28, p96, p120|Middle Cambrian|Middle Cambrian|Boucher (1991). Eastern Warburton Basin.|||||Basalt and agglomerate.|12-NOV-15
30532|Jena Basalt|67536|6|Mentioned|Map Legend|||Warburton Basin.|||||Within-plate amygdaloidal basalt, hyaloclastite, porphyritic and trachytic basalt.|
30532|Jena Basalt|68731|6|Mentioned|p170 Fig 3.83|Middle Cambrian|Middle Cambrian|||||||
30532|Jena Basalt|69728|6|Mentioned|p285, 298|||Warburton Basin. Has a within-plate continental geochemical affinity. Name appears in quotation marks.||Mooracoochie Volcanics.||||
30532|Jena Basalt|69982|3|Fully described|p22-23, p10, p17-19, p45, p149-150, p220|Late Cambrian|Early Cambrian|See also p223, Appendix 1. Informally named by Boucher (1991). Warburton Basin. Type well is Jena 1, over the interval 1570.6 m to a total depth of 1600.81 m. Base of the unit has not yet been penetrated. Has been reworked into turbidites of the Dullingari Group. Brief thin section descriptions. Appears as 'Jena basalt' on p64. Composite log shown. Bedding dip angles in wells listed. Details of wells with hydrocarbon shows.||||Overlies Mooracoochie Volcanics. Is intercalated with Kalladeina and Lycosa Formations.|Three facies: massive, fine-grained, amygdaloidal basalt; basaltic hyaloclastite or brecciated basalt lavas intercalated with and resedimented within deep-water limestone; porphyritic and trachytic basalt.|12-NOV-15
81775|Jenners Supersuite|67323|6|Mentioned|Eastern Australia Time-Space Plot|||Southern Gawler Craton.||||||
73754|Jessieu Metadolerite|63398|5|Briefly described|p669, p670 Fig. 6d|Paleoproterozoic|Paleoproterozoic|Age: ca 1850Ma. Mafic rocks. ||||||07-NOV-08
68744|Jussieu Metadolerite|60958|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Composed of hornblende, plagioclase, sphene and minor quartz. Foliated. Intrudes Gleesons Landing Granite. Of the Donnington Suite. Geological Province: Gawler Craton.||||||07-NOV-08
68744|Jussieu Metadolerite|61070|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Donington Suite. Mafic dykes, variably recrystallised to hornblende granulite and amphibolite facies. Geological Province: Gawler Craton.||||||12-JAN-10
68744|Jussieu Metadolerite|61121|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Comprises hornblende, plagioclase, sphene and minor quartz; foliated.  Intrudes Gleesons Landing Granite with back-veining texture. Geological Province: Gawler Craton.||||||07-NOV-08
68744|Jussieu Metadolerite|65375|5|Briefly described|pp13-14, p18.|Paleoproterozoic|Paleoproterozoic|Syn-Gleesons Landing Granite in age. Boudinage and back-veining common. Slightly high (>51%) SiO2.|1850 Ma.|Unit in Donington Suite.||||
68744|Jussieu Metadolerite|66302|6|Mentioned|p28|||||||Intrudes the Donington Suite.||
68744|Jussieu Metadolerite|68131|5|Briefly described|p43, p47-48|||Repeatedly mis-spelt as Jusseiu.||Donington Suite.||||
68744|Jussieu Metadolerite|69213|6|Mentioned|p25 Fig. 2|||||||||
68744|Jussieu Metadolerite|73026|5|Briefly described|p5|||Occurs as abundant dykes.||Donington Suite|||Metadolerite.|
68744|Jussieu Metadolerite|73027|6|Mentioned|p5, p19|Palaeoproterozoic|Palaeoproterozoic|Occurs as abundant dykes.||Donington Suite||||
68744|Jussieu Metadolerite|73122|5|Briefly described|p20, 23, 28|||Folded by the 1850-1843 Ma Cornian Orogeny. Appears also as Jussieu Metadolerites/Jussieu Metadolerite Dykes/Jussieu Dykes.|||||Mafic dykes.|
68744|Jussieu Metadolerite|73493|5|Briefly described|p712-713|||Co-magmatic and petrogenetically linked with Donington Suite.|||||Mafic rocks.|
68744|Jussieu Metadolerite|73525|5|Briefly described|p19 Fig.13|||Olympic Domain.||Donington Suite|||Mafic intrusive.|
68744|Jussieu Metadolerite|73634|6|Mentioned|p3-4, 6-7, 17|||Hoek and Schaefer, (1998). Jussieu Peninsula, Gawler Craton. These dykes provided sites for strain localisation. More often referred to in the text as Jussieu Metadolerite Dykes or, less formally, as Jussieu dyke(s).||||Is intruded by Tournefort Metadolerite dykes.||
27808|Kadlunga Slate|22889|6|Mentioned|p37|Adelaidean|Adelaidean|Parent - Belair Subgroup.||||||
27808|Kadlunga Slate|30801|6|Mentioned|p5|||Burra Group. Table P5-6||||||
27808|Kadlunga Slate|30807|6|Mentioned|p103|||Suggested map symbol||||||
27808|Kadlunga Slate|32510|6|Mentioned|Table 1|||||||||
27808|Kadlunga Slate|33474|6|Mentioned|Fig.2|||||||||
27808|Kadlunga Slate|34587|5|Briefly described|p36|||||||||
27808|Kadlunga Slate|39344|6|Mentioned|Map legend|Precambrian|Precambrian|Sturtian||||||
27808|Kadlunga Slate|41404|4|Described|p121|||||||||
27808|Kadlunga Slate|42098|5|Briefly described|Table 2 P54|||||||||
27808|Kadlunga Slate|42222|6|Mentioned|p15|||||||||
27808|Kadlunga Slate|43052|5|Briefly described|p183,Table 6.1|||of Belair Subgroup||||||
27808|Kadlunga Slate|44659|5|Briefly described|map legend|||Sturtian, lithology.||||||
27808|Kadlunga Slate|44690|4|Described|map legend|||Geol. Atlas Series. (I/54-5). Sturtian.||||||
27808|Kadlunga Slate|62724|5|Briefly described|p17 Fig. 4|Sturtian|Sturtian|Of the Belair Subgroup (Burra Group). Intertonguing Sandstone and siltstone. Transitional over Gilbert Range Quartzite.||||||07-FEB-11
27808|Kadlunga Slate|70405|5|Briefly described|p50|Cryogenian|Cryogenian|||Belair Subgroup|||Siltstone. Exposed thickness of 100m.|
27808|Kadlunga Slate|70819|5|Briefly described|p13, 28|Neoproterozoic|Neoproterozoic|Clare Valley.||Belair Subgroup.||Overlies Gilbert Range Quartzite. Is overlain disconformably by Appila Tillite.|Dark grey siltstones.|
27808|Kadlunga Slate|71237|14|Not recorded|p9, 17|||||||||
27808|Kadlunga Slate|74367|6|Mentioned|p7 Fig.6|||||Belair Subgroup||||
75514|Kalabity Supersuite|70405|5|Briefly described|p1, p12 figure 4, p33|Paleoproterozoic|Paleoproterozoic||1710 Ma - 1720 Ma||Includes Basso Suite,Bumbumbie Suite||Bimodal igneous rocks.|
24326|Kalachalpa Formation|22889|6|Mentioned|p35|Adelaidean|Adelaidean|Parent - Bungarider Subgroup.||||||
24326|Kalachalpa Formation|23054|5|Briefly described|p11-2,14|||||||||
24326|Kalachalpa Formation|36733|2|Defined|p71|Adelaidean|Adelaidean|See also P45.||||||
24326|Kalachalpa Formation|38108|6|Mentioned|Table 1|||||||||
24326|Kalachalpa Formation|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Torrensian||||||
24326|Kalachalpa Formation|40856|5|Briefly described|p312|||||||||
24326|Kalachalpa Formation|41404|4|Described|p116|||||||||
24326|Kalachalpa Formation|42222|5|Briefly described|p14|||||||||
24326|Kalachalpa Formation|43052|5|Briefly described|p183,Table 6.2|||||||||
24326|Kalachalpa Formation|44289|5|Briefly described|Map Legend||Neoproterozoic|||||||
24326|Kalachalpa Formation|64796|5|Briefly described|p189 fig 7, p191 Fig.9, p197 Tb.5  |Neoproterozoic|Neoproterozoic|See also p198 Tb.6, p200 Fig.10, p202-204, p206.||Unit in Burra Group.|||Contains 174m thick white arenite at top; topped by tillite.|
24326|Kalachalpa Formation|64797|6|Mentioned|p160 Fig.8, p161 Tb.4|||S-isotope data.||Unit in Burra Group.||||
24326|Kalachalpa Formation|65365|5|Briefly described|p5, p6 Fig. 2, p7, 9 Fig. 3, p11|Cryogenian|Cryogenian|Of Burra Group. Peake and Denison Ranges.||||||19-MAR-12
75724|Kalkarindji Suite|68193|5|Briefly described|p44|||Kalkarindji Province. Heavily explored, geophysically anomalous locations have all proved negative for diamonds.|||||Basalts.|
75724|Kalkarindji Suite|69417|5|Briefly described|p2:6|Early Cambrian|Early Cambrian|Kalkarindji Province.|507 +/- 4 Ma.|||||12-JUL-16
75724|Kalkarindji Suite|69420|6|Mentioned|p5:81|Early Cambrian|Early Cambrian|Covered most of the North Australian Craton.||||||12-JUL-16
75724|Kalkarindji Suite|69422|6|Mentioned|p7:2 Fig.7.2|Cambrian|Cambrian|Kalkarindji Province.||||||12-JUL-16
75724|Kalkarindji Suite|69429|5|Briefly described|p14:4 Fig.14.7|Early Cambrian|Early Cambrian|Kalkarindji Province.|||||Includes basalt flows.|12-JUL-16
75724|Kalkarindji Suite|69432|5|Briefly described|p17:2, 4|Early Cambrian|Early Cambrian|Kalkarindji Province.||||Overlies Birrindudu Group.||12-JUL-16
75724|Kalkarindji Suite|69444|6|Mentioned|p29:5-6|||Shares geochemical similarities with the Indiana Suite in the southeastern Harts Range.|c.508 Ma.|||||12-JUL-16
75724|Kalkarindji Suite|69445|2|Defined|p30:1-12, 16-17|||Glass and Munson in Ahmad and Munson (2013). New name, after Kalkarindji township. Formerly Kalkarindji Volcanic Group of Kruse in Rawlings et al. (2008). Includes the igneous component of Kalkarindji Large Igneous Province, formerly the Kalkarinji (later revised by Glass and Phillip 2006) Continental Flood Basalt Province of Glass (2002). The definition excludes the minor intercalated sedimentary components of the former Group; they are included within the constituent Formations. 60-1100m thick; 760m thick at the type locality at Purnululu National Park, from WGS84 52K 426414mE 8078661mN to 428989mE 8079851mN. Four reference sections are detailed as are type sections for constituent Formations. Geochemistry and petrology described. Correlated with Mount Wright Volcanics and Cymbric Vale Formation (both Gnalta Group), Truro Volcanics, possibly Mooracoochie Volcanics.|||Antrim Plateau, Helen Springs, Colless, Table Hill Volcanics; Milliwindi Dolerite; Mount Ramsay dolerite.|Unconformably overlies Mount Forster Sandstone. Is overlain unconformably by Headleys, Montejinni, Tindall, Top Springs, Thorntonia Limestones; Tarrara, Gum Ridge, Wonarah Formations.|Tholeiitic basalt and dolerite with massive, porphyritic, partly vesicular (flow tops), amygdaloidal glomeroporphyritic textures, microdolerite, basaltic flow breccia, peperite, pyroclastic deposits.|12-JUL-16
75724|Kalkarindji Suite|69917|6|Mentioned|p175|||Geochemically similar to Coggans Gabbro.|ca 508 Ma|||||
75724|Kalkarindji Suite|70866|5|Briefly described|Map legend.|Cambrian|Cambrian|Kalkarindji Province.|||Includes Antrim Plateau Volcanics, Jindare Formation.|||01-MAR-18
75724|Kalkarindji Suite|70968|5|Briefly described|p6, p51, p100, p131, p137|Early Cambrian|Early Cambrian||||Helen Springs Volcanics.|Unconformably overlies Roper Group.|Basaltic volcanism.|
75724|Kalkarindji Suite|71267|6|Mentioned|1M_geologyp12_lut.csv|||||||||
75724|Kalkarindji Suite|71779|5|Briefly described|p5|Early Cambrian|Early Cambrian|||||Unconformably overlies the Roper Group.||24-SEP-18
75724|Kalkarindji Suite|71893|5|Briefly described|p41, p948|Cambrian|Cambrian|McArthur Basin.|507 +/- 4 Ma (Ar-Ar, Glass and Phillips 2006)|||Overlies the Jamison sandstone.||
75724|Kalkarindji Suite|73083|6|Mentioned|p: 1, 3, 12, 14-15, 17-18, 21, 24-25...|Cambrian|Cambrian|Strongly magnetic. Part of the Kalkarindji Continental Flood Basalt Province. Marked as Ebk on solid geology maps. Widespread in the Georgina Basin sequence. Associated with possible feeder dykes (labelled Ed - Cambrian dolerite) and altered Cambrian basalt is labelled Ebkl. [Written as Kalkarindji Igneous Suite on p30]. More locations p: 28-31, 34-35, 38, 42-45, 48-49, 55.||||Underlain by Kinevans Sandstone.|Basalt and agglomerate.|
24329|Kalladeina Formation|13497|5|Briefly described|p55,. p114|Early Ordovician|Middle Cambrian|Warburton Basin.||||Overlies the Mooracoochie Volcanics.||
24329|Kalladeina Formation|23154|4|Described|Map Legend|Cambrian|Cambrian|Geological Province - Warburton Basin.  Unit contains trilobites, molluscs, brachiopods, and calcified cyanobacteria.||||||
24329|Kalladeina Formation|23155|4|Described|p8|Ordovician|Cambrian|Thickness varies from 30 to 110 m.||||||
24329|Kalladeina Formation|38661|2|Defined|p5|Datsonian|Middle Cambrian|Early Middle Cambrian (Floran)-late Late Cambrian(Payntonian-Datsonian).||||||
24329|Kalladeina Formation|40642|4|Described|p169|||Mention p161.||||||06-FEB-07
24329|Kalladeina Formation|40830|6|Mentioned|p8|||||||||
24329|Kalladeina Formation|42064|4|Described|p166|||See also p178.||||||06-FEB-07
24329|Kalladeina Formation|42357|5|Briefly described|p4|||||||||
24329|Kalladeina Formation|42746|4|Described|p3, Fig.2 p5|||||||||
24329|Kalladeina Formation|43201|6|Mentioned|p8|||||||||
24329|Kalladeina Formation|44133|5|Briefly described|p4 Fig. 7.2, 31-32|Early Ordovician|Early Cambrian|Geological Province: Eastern Warburton Basin. Dolomitised limestone.||||||
24329|Kalladeina Formation|62537|6|Mentioned|p191 Fig.2. |Early Ordovician|Middle Cambrian|Warburton Basin.||||||
24329|Kalladeina Formation|63056|5|Briefly described|p81 Fig. 2|Late Cambrian|Middle Cambrian|Thickness: >1620m. Geological Province: Warburton Basin. Shallow shelfal deposits: ooid grainstone, dolomitised in places.||||||06-FEB-07
24329|Kalladeina Formation|63978|5|Briefly described|p5|Early Ordovician|Middle Cambrian|Overlain by the Innamincka Formation. Mixed carbonate-siliciclastic unit. Upper section passes laterally into the Dullingari Group. Geological province: Warburton Basin.||||||07-FEB-11
24329|Kalladeina Formation|65337|5|Briefly described|p95.|Middle Cambrian|Middle Cambrian|||||Unconformably overlies Mooracoochie Volcanics.||
24329|Kalladeina Formation|65489|4|Described|p14, p28-29, p32, p34-36, p39-40, p96|Early Ordovician|Middle Cambrian|See also p118-121. Gatehouse (1983). Eastern Warburton Basin. Type section in Kalladeina 1. Over 1700m thick. Compressed and uplifted during the Ordovician, possibly related to the Delamerian Orogeny. Potential reservoir sandstones. The Challum 19 well in SW Queensland flowed gas in 2001.|||Includes Coongie Limestone Member.|Unconformably overlies Diamond Bog Dolomite and Mooracoochie Volcanics. Is intercalated with Jena Basalt. Is overlain by Innamincka Formation.|Limestone (ooid grainstone), locally dolomitised; dolomite, shale, siltstone, sandstone and minor tuffs.|
24329|Kalladeina Formation|65925|5|Briefly described|Appendix 2.||||||||Limestone; ooid-oncolite packstone, recrystallised with silicified trilobites.|
24329|Kalladeina Formation|67402|4|Described|p104, p104 fig CPR23, p239, p260, p261|Lancefieldian|Ordian|Warburton Basin. Unsuitable for the injection of carbon dioxide. Deposited in a shelf-basin floor setting. Up to 1660m thick.  ||||Overlies the Diamond Bog Dolomite. Overlain by the Pando Formation and the Innamincka Formation. Grades laterally into the Dullingari Group.|Feldspathic sandstone and shale, pyritic shale, minor siltstone.|
24329|Kalladeina Formation|67536|6|Mentioned|Map Legend|||Warburton Basin.|||||Shelf limestone, dolomite, siltstone, shale and sandstone.|01-APR-14
24329|Kalladeina Formation|68731|5|Briefly described|p115, p168, p170 Fig 3.83, p171|Late Cambrian|Late Cambrian|Warburton Basin. Shallow marine depositional environment. > 1620 m thick.||||Interfingers with the basinal shale of the Dullingari Group. Unconformably underlain by the Diamond Bog Dolomite. Partly overlain by the Pando Formation.|Shallow shelf (ooid grainstone, dolomitised in places), slope to basinal carbonate.|15-JUL-14
24329|Kalladeina Formation|69019|6|Mentioned|p145-146.|||Warburton Basin. Steeply-dipping.||||Intruded by Big Lake Suite granite.||
24329|Kalladeina Formation|69023|5|Briefly described|p78, p149|||Warburton Basin. Steeply dipping; contact metamorphosed by granite plutons of Big Lake Suite.||||Is intruded by Big Lake Suite.||
24329|Kalladeina Formation|69445|5|Briefly described|p30:17|Middle Cambrian|Middle Cambrian|Warburton Basin.||||Unconformably overlies Mooracoochie Volcanics.||12-JUL-16
24329|Kalladeina Formation|69449|5|Briefly described|p34:2 Fig.34.2|Cambrian|Cambrian|Eastern Warburton Basin.||||Unconformably overlies Mooracoochie Volcanics. Is overlain by Dullingari Group.||12-JUL-16
24329|Kalladeina Formation|69573|6|Mentioned|p656-657, 659, 661-662, 667, 670|||Warburton Basin; subsurface. Features Cambrian Stage 5 fossil sites.||||||
24329|Kalladeina Formation|69673|6|Mentioned|p149 fig 120|||||||||
24329|Kalladeina Formation|69982|3|Fully described|p21-23, p10, p13, p17-19, p29, p45, p51|Early Ordovician|Middle Cambrian|See also p60-61, p148, p158, p161, p194, p220, p223-224, Appendix 1. Gatehouse (1983). Warburton Basin. Type well is Kalladeina 1 over the interval 1956.82 - 3580.20 m (1623.4 m thick). Here divided into three informal members, one named. Wireline log and simplified lithologies detailed. Interpreted as deep-water lime mudstone and shale, a lateral facies variation of the Lycosa Formation. Richly fossiliferous. Reservoir attributes described. Brief thin section descriptions. Composite logs shown. Bedding dip angles in wells listed. Details of wells with hydrocarbon shows.||Possibly part of Dullingari Group? But described separately.|Includes Coongie Limestone Member (informal).|Is intercalated with Jena Basalt. Is thrust faulted over Innamincka Formation.|Limestone, dolomite, shale, siltstone and sandstone; minor tuffs.|12-NOV-15
24329|Kalladeina Formation|70749|5|Briefly described|p43-44, p54|Ordovician|Cambrian|Warburton Basin. Extends into undercover Thomson Orogen. Deep marine: starved basin sediments (also described as shallow shelf carbonates).||||Is overlain by Innamincka Formation.|Finely interlaminated black pyritic shale, lime mudstone, limestone and grey to white calcareous siltstone to sandstone.|
24329|Kalladeina Formation|70823|5|Briefly described|p35|Ordovician|Cambrian|Warburton Basin. Deposited in a shallow shelf or slope marine environment.|||||Carbonates.|
24329|Kalladeina Formation|71283|5|Briefly described|p471, p472 Fig.2, p473|Ordovician|Cambrian|Gatehouse (1983, 1986). Warburton Basin. Stratigraphic and gamma-ray log. Trilobite species described in detail.|||||Limestone, dolomite, shale, siltstone, sandstone and minor tuff.|
24329|Kalladeina Formation|71342|6|Mentioned|Ch10 p20|Cambrian|Cambrian|Warburton Basin.||||||
24329|Kalladeina Formation|72478|6|Mentioned|Fig. 7 p70|||||||||
24329|Kalladeina Formation|73167|6|Mentioned|p669, p672 Tb. 1|||Warburton Basin.|||||Limestone-rich.|
24329|Kalladeina Formation|73244|6|Mentioned|p86|Cambrian|Cambrian|Warburton Basin. Shallow shelf environment. Source rock.||||||
24329|Kalladeina Formation|73479|5|Briefly described|p156|Cambrian|Cambrian|Warburton Basin. Shallow shelf depositional environment.|ca 508-485 Ma||Coongie Limestone Member|Overlies Diamond Bog Dolomite, underlies Pando Formation||
78312|Kanaka beds|68715|6|Mentioned|p31 Fig.5, p32 Fig.6|Eocene|Eocene|Pirie Basin. Middle to Late Eocene.||||||
78312|Kanaka beds|71413|5|Briefly described|p31, 32|Eocene|Eocene|Includes Plumbush U deposit.||||Overlies Samphire granite.||
76223|Kandramooka Member|72429|3|Fully described|p952, p956, p965-966, p968, p970-971|Lower Cambrian|Lower Cambrian|Mount Chambers Gorge, eastern Flinders Ranges. This is an important reef-megabreccia horizon that is mapped as both a lower section [see lithology section] which is up to 49m thick and an upper section described as follows:  Massive, clean, light to dark grey archaeocyathan limestones with silty interbeds and thin siliciclastic grit stringers. Up to 32m thick in measured section. Records change in depositional environment towards the end of the Hawker Group. Depositional environment is interpreted as a shallow-marine carbonate platform margin, draped with extensive low-profile archaeocyath meadows. Megabreccia was interpreted to have formed gradually by persistent wave or tidal current attrition of a thin carbonate sheet or terrace with residual slabs accumulating as ablation rubble on the shallow seafloor or in broad bypass channels, to be vigorously reworked by tidal currents. Features fossil archaeocyaths that are commonly large, abundant and mostly intact and associated with small stromatolite mounds. Calcimicrobes Renalcis, Girvanella and Epiphyton formed mats, rinds, crusts and complex intergrowths with the archaeocyaths. Small brachiopods, hyoliths and possible trilobites are present. Constituent subfacies are discussed in detail, including fossil assemblages, depositional environments and lithologies.||Moorowie Formation||Overlies the Wookata Shale Member. Underlies the Pack Creek Member.|Megabreccia is massive, peloidal to archaeocyathan limestones in the east with ooid grainstone lenses, passing west to unsorted boulder conglomerates of clean grey limestone clasts to 3m in a quartz-granule rich silty carbonate matrix.|
28634|Kanmantoo Group|7992|6|Mentioned|165|Ordovician|Cambrian|||||||
28634|Kanmantoo Group|9124|5|Briefly described|Map Legend|Cambrian|Cambrian|||||||
28634|Kanmantoo Group|12781|6|Mentioned|p386|Paleozoic|Paleozoic|Basement to Otway Basin.||||Is overlain unconformably by Casterton Formation.||
28634|Kanmantoo Group|22458|5|Briefly described|p523||Cambrian|||||||
28634|Kanmantoo Group|22492|5|Briefly described|31|Cambrian|Cambrian|||||||
28634|Kanmantoo Group|22531|6|Mentioned|p2|||||||||
28634|Kanmantoo Group|22573|4|Described|p 47, Fig 1||Cambrian|Minimum thickness: >8km.||||||04-MAY-10
28634|Kanmantoo Group|22580|6|Mentioned|p89|Cambrian|Cambrian|||||||
28634|Kanmantoo Group|22581|5|Briefly described|Fig.2,p37||Cambrian|In the Kanmantoo Basin.||||||17-JAN-07
28634|Kanmantoo Group|22603|5|Briefly described|p99||Early Cambrian|Age: 540 Ma (?)||||||17-JAN-07
28634|Kanmantoo Group|22628|6|Mentioned|p109,p112|||||||||
28634|Kanmantoo Group|22634|5|Briefly described|p506|Cambrian|Neoproterozoic|||||||
28634|Kanmantoo Group|22643|4|Described|p186, fig3,6,7|Early Cambrian|Early Cambrian|||||||
28634|Kanmantoo Group|22671|5|Briefly described|p848-49|||Overlies Heatherdale Shale. Geological Province: Kanmantoo Fold Belt.||||||18-JAN-06
28634|Kanmantoo Group|22708|6|Mentioned|p207|||||||||
28634|Kanmantoo Group|22719|6|Mentioned|p487|||||||||
28634|Kanmantoo Group|22726|6|Mentioned|p233,235||Early Cambrian|||||||
28634|Kanmantoo Group|22755|4|Described|p547, Fig.1 p548||Early Cambrian|In the Stansbury Basin. See also p548.||||||17-JAN-07
28634|Kanmantoo Group|22766|4|Described|Fig.2 p561, p562|Early Cambrian|Early Cambrian|||||||
28634|Kanmantoo Group|22772|5|Briefly described|Table 13.1|Middle Cambrian|Early Cambrian|||||||
28634|Kanmantoo Group|22840|5|Briefly described|P37||Cambrian|||||||
28634|Kanmantoo Group|22848|5|Briefly described|36|||||||||
28634|Kanmantoo Group|22857|5|Briefly described|Tb 13.1 (insert p70-71), p75, p94, p96|Middle Cambrian|Early Cambrian|Of the Moralana Supergroup. Correlate with Teltawongee beds. Max. thickness: 9km. Geological Province: Kanmantoo Trough. See also p99 and p405 App.1 Tb.A1.4.||||||04-MAY-10
28634|Kanmantoo Group|22858|6|Mentioned|p75,Fig14.8p96,96||Early Cambrian|Max Age: 526 (+/-) 6 Ma.||||||
28634|Kanmantoo Group|22869|6|Mentioned|P40|||||||||
28634|Kanmantoo Group|22875|6|Mentioned|p25|||||||||
28634|Kanmantoo Group|22933|6|Mentioned|p10|||||||||
28634|Kanmantoo Group|22938|6|Mentioned|p235||Cambrian|||||||
28634|Kanmantoo Group|22944|5|Briefly described|Fig3|Tithonian||||||||
28634|Kanmantoo Group|22945|5|Briefly described|p8|Cambrian|Cambrian|Mentioned under - Area C geology.||||||
28634|Kanmantoo Group|22951|6|Mentioned|p55|||||||||
28634|Kanmantoo Group|23019|6|Mentioned|p617|||||||||
28634|Kanmantoo Group|23022|6|Mentioned|p1803|||||||||
28634|Kanmantoo Group|23023|6|Mentioned|p1797,1799-1800|||||||||
28634|Kanmantoo Group|23226|6|Mentioned|p895|||Transgressive to Mannum Formation.||||||
28634|Kanmantoo Group|23309|5|Briefly described|p19, 26, 40, 46, 195.|||||||||
28634|Kanmantoo Group|23317|5|Briefly described|377|Early Cambrian|Early Cambrian|Includes clastic turbidites. Geological Province: Adelaide Fold Belt.||||||04-MAY-10
28634|Kanmantoo Group|23319|5|Briefly described|p407|Early Cambrian|Early Cambrian|||||||07-FEB-07
28634|Kanmantoo Group|23539|4|Described|p 466- 467|||||||||
28634|Kanmantoo Group|23564|6|Mentioned|p1444|||||||||
28634|Kanmantoo Group|23731|6|Mentioned|p43|||||||||
28634|Kanmantoo Group|23818|4|Described|p51 Fig.16, p99|Cambrian|Cambrian|Underlain by Barossa Complex, Adelaidean Group and Hawker Group (unconformable). Max. thickness: 60 000 ft.||||||17-JAN-07
28634|Kanmantoo Group|23824|5|Briefly described|p100 Fig 2|Early Devonian|Cambrian|Geological Province: Great Australian Bight Basin.||||||
28634|Kanmantoo Group|23827|5|Briefly described|p260|Cambrian|Cambrian|||||||
28634|Kanmantoo Group|23854|5|Briefly described|p863|Middle Cambrian|Early Cambrian|||||||
28634|Kanmantoo Group|23869|5|Briefly described|p15 Fig. 3|Cambrian|Cambrian|||||||
28634|Kanmantoo Group|23932|5|Briefly described|p667|Early Cambrian|Early Cambrian|Geological Province: Adelaide Fold Belt.||||||
28634|Kanmantoo Group|23981|5|Briefly described|p8-9 Fig. 4|Early Cambrian|Early Cambrian|Thick sequence of siliciclastics. Disconformably overlies Normanville group. Thickness>8000m. Geological Province: Stansbury Basin (Fleurieu Peninsula).||||||12-FEB-07
28634|Kanmantoo Group|23991|5|Briefly described|p188 Fig.1|Cambrian|Cambrian|||||||
28634|Kanmantoo Group|23996|5|Briefly described|p352 Fig.1|Cambrian|Cambrian|Geological Province: Adelaid Fold Belt.||||||07-MAR-05
28634|Kanmantoo Group|24102|5|Briefly described|p131, p132 Fig.2|Cambrian|Cambrian|Age: ~520 Ma.||||||30-NOV-04
28634|Kanmantoo Group|24263|4|Described|p1384||Cambrian|Geological Province: Wonominta Block.||||||17-JAN-07
28634|Kanmantoo Group|24314|5|Briefly described|p61 Fig.2||Paleozoic|Geological Province: Otway Basin.||||||07-NOV-08
28634|Kanmantoo Group|24361|6|Mentioned|p50|Cambrian|Cambrian|||||||
28634|Kanmantoo Group|24362|6|Mentioned|p42|Cambrian|Cambrian|||||||
28634|Kanmantoo Group|24381|6|Mentioned|p58|||||||||
28634|Kanmantoo Group|24425|6|Mentioned|p16|||Fractured rock aquifer.||||||
28634|Kanmantoo Group|24465|4|Described|p343|Middle Cambrian|Early Cambrian|Overlies Normanville Group.  Geological Province: Stansbury Basin.||||||19-JAN-05
28634|Kanmantoo Group|24509|5|Briefly described|p39, p41 Fig. 2b|Cambrian|Cambrian|Metasedimentary rock. Interbedded with Teal Flat Volcanics.||||||
28634|Kanmantoo Group|24551|5|Briefly described|p74|Cambrian|Cambrian|Of the Moralana Supergroup in SA.||||||
28634|Kanmantoo Group|24566|5|Briefly described|p110, p111|Cambrian|Cambrian|||||||
28634|Kanmantoo Group|24599|5|Briefly described|p494|||Geological Province: Adelaide Fold Belt.||||||
28634|Kanmantoo Group|24604|5|Briefly described|p907 Fig. 4|Cambrian|Cambrian|Group is Gp in text.||||||
28634|Kanmantoo Group|29395|6|Mentioned|p1|||||||||
28634|Kanmantoo Group|29406|6|Mentioned|p51|||||||||
28634|Kanmantoo Group|29474|6|Mentioned|p7|||[Originally entered for NT. CEBMar95]||||||
28634|Kanmantoo Group|29591|6|Mentioned|p103|||||||||
28634|Kanmantoo Group|29665|6|Mentioned|p77|||||||||
28634|Kanmantoo Group|29697|6|Mentioned|p7|||||||||
28634|Kanmantoo Group|29836|4|Described|p89|||||||||
28634|Kanmantoo Group|29872|6|Mentioned|p77|||||||||
28634|Kanmantoo Group|30051|6|Mentioned|Fig.1|||Middle Cambrian age.||||||
28634|Kanmantoo Group|30052|5|Briefly described|p91|||Middle Cambrian age.||||||
28634|Kanmantoo Group|30085|6|Mentioned|p132|||Geological Plan on P132. Cambrian age.||||||
28634|Kanmantoo Group|30329|6|Mentioned|p30|||On table P30||||||
28634|Kanmantoo Group|30377|4|Described|p203|||See also p204-207.||||||17-JAN-07
28634|Kanmantoo Group|30378|6|Mentioned|p431|||Lower Cambrian age.||||||
28634|Kanmantoo Group|30379|5|Briefly described|p90|||Cambrian age||||||
28634|Kanmantoo Group|30380|6|Mentioned|Table 1|||Correlation||||||
28634|Kanmantoo Group|30381|4|Described|p213|||See also p214-251.||||||17-JAN-07
28634|Kanmantoo Group|30382|6|Mentioned|p388|||||||||
28634|Kanmantoo Group|30398|5|Briefly described|p259|||||||||
28634|Kanmantoo Group|30753|6|Mentioned|Table 2|||Lower Permian age||||||
28634|Kanmantoo Group|30754|6|Mentioned|p12|||Stratigraphic table||||||
28634|Kanmantoo Group|30758|5|Briefly described|p65|||Schist as source of aggregate P66. Favourable foundation conditions P70||||||
28634|Kanmantoo Group|30783|5|Briefly described|p12|||Sediments discussed||||||
28634|Kanmantoo Group|30801|6|Mentioned|p5|||Table P5-6||||||
28634|Kanmantoo Group|30805|6|Mentioned|p4|||||||||
28634|Kanmantoo Group|30807|6|Mentioned|p102|||Suggested map symbol||||||
28634|Kanmantoo Group|31292|6|Mentioned|p1|||Cambrian||||||
28634|Kanmantoo Group|31314|6|Mentioned|p102|||||||||
28634|Kanmantoo Group|31321|5|Briefly described|p15|||See also P16. Map. Mineral deposits||||||
28634|Kanmantoo Group|31322|6|Mentioned|p23|||M. Cambrian. Stratigraphy||||||
28634|Kanmantoo Group|31577|5|Briefly described|p76|||Cambrian||||||
28634|Kanmantoo Group|31851|6|Mentioned|Fig. 2|||||||||
28634|Kanmantoo Group|31923|6|Mentioned|p11|||||||||
28634|Kanmantoo Group|31999|6|Mentioned|p127|||||||||
28634|Kanmantoo Group|32146|6|Mentioned|p369|||||||||
28634|Kanmantoo Group|32161|6|Mentioned|p55|||Basement||||||
28634|Kanmantoo Group|32194|6|Mentioned|p311|||||||||
28634|Kanmantoo Group|32196|4|Described|p149|||||||||
28634|Kanmantoo Group|32321|6|Mentioned|p82|||||||||
28634|Kanmantoo Group|32323|5|Briefly described|p9|||Petrology||||||
28634|Kanmantoo Group|32401|6|Mentioned|p103|||||||||
28634|Kanmantoo Group|32404|6|Mentioned|p18|||||||||
28634|Kanmantoo Group|32432|6|Mentioned|Fig.2|||See also Table 1||||||
28634|Kanmantoo Group|32433|6|Mentioned|p80|||See also Table 2||||||
28634|Kanmantoo Group|32439|6|Mentioned|p99|||||||||
28634|Kanmantoo Group|32457|6|Mentioned|p88|||||||||
28634|Kanmantoo Group|32547|4|Described|p60|||L.-M. Camb.||||||
28634|Kanmantoo Group|32791|6|Mentioned|p11|||||||||
28634|Kanmantoo Group|33224|6|Mentioned|p48|||Photo Fig.35||||||
28634|Kanmantoo Group|33236|6|Mentioned|p24|||L. - M.Camb.||||||
28634|Kanmantoo Group|33311|6|Mentioned|p50|||||||||
28634|Kanmantoo Group|33332|3|Fully described|p11|||Lower Cambrian. See also Figs. 3 and 4.||||||05-MAR-08
28634|Kanmantoo Group|33468|6|Mentioned|p217|||||||||
28634|Kanmantoo Group|33471|4|Described|p555|||||||||
28634|Kanmantoo Group|33472|6|Mentioned|p470|||||||||
28634|Kanmantoo Group|33474|6|Mentioned|Fig.1|||||||||
28634|Kanmantoo Group|33488|6|Mentioned|p8|||||||||
28634|Kanmantoo Group|33490|4|Described|p10|||Cambrian?||||||
28634|Kanmantoo Group|33625|6|Mentioned|p198|||||||||
28634|Kanmantoo Group|33634|6|Mentioned|p561|||||||||
28634|Kanmantoo Group|33798|6|Mentioned|p98|||||||||
28634|Kanmantoo Group|33834|5|Briefly described|p7|||||||||
28634|Kanmantoo Group|33936|6|Mentioned|Fig.1a|||||||||
28634|Kanmantoo Group|33998|6|Mentioned|p25|||Cambrian||||||
28634|Kanmantoo Group|34029|5|Briefly described|Table 1|||?Cambrian||||||
28634|Kanmantoo Group|34185|6|Mentioned|p129|||||||||
28634|Kanmantoo Group|34195|6|Mentioned|p1|||Cambrian ?||||||
28634|Kanmantoo Group|34248|5|Briefly described|p113|||Palaeozoic||||||
28634|Kanmantoo Group|34265|6|Mentioned|p242|||Camb.||||||
28634|Kanmantoo Group|34287|6|Mentioned|p59|||||||||
28634|Kanmantoo Group|34296|4|Described|p97|||||||||
28634|Kanmantoo Group|34308|6|Mentioned|p181|||||||||
28634|Kanmantoo Group|34497|6|Mentioned|p60|||Cambrian. See P61||||||
28634|Kanmantoo Group|34535|6|Mentioned|Fig.16|||Camb.||||||
28634|Kanmantoo Group|34536|6|Mentioned|Map legend|Middle Cambrian|Early Cambrian|Lower to Middle Cambrian||||||
28634|Kanmantoo Group|34598|6|Mentioned|p20|||Cambrian||||||
28634|Kanmantoo Group|34612|3|Fully described|p102|||See also Fig.32.||||||05-MAR-08
28634|Kanmantoo Group|34617|6|Mentioned|p2|||||||||
28634|Kanmantoo Group|34719|6|Mentioned|p374|||||||||
28634|Kanmantoo Group|34760|6|Mentioned|Fig.1|||||||||
28634|Kanmantoo Group|34812|6|Mentioned|Table 9|||||||||
28634|Kanmantoo Group|34933|6|Mentioned|p60|||||||||
28634|Kanmantoo Group|34941|6|Mentioned|p234|||||||||
28634|Kanmantoo Group|35027|6|Mentioned|p385|||||||||
28634|Kanmantoo Group|35089|4|Described|p203|||Discussed throughout.||||||
28634|Kanmantoo Group|35092|6|Mentioned|p108|||||||||
28634|Kanmantoo Group|35099|6|Mentioned|p332|||||||||
28634|Kanmantoo Group|35175|6|Mentioned|p1166|||||||||
28634|Kanmantoo Group|35200|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
28634|Kanmantoo Group|35232|6|Mentioned|p5|||See also Table.1||||||
28634|Kanmantoo Group|35255|6|Mentioned|Fig.8|||||||||
28634|Kanmantoo Group|35358|5|Briefly described|p8|||||||||
28634|Kanmantoo Group|35565|6|Mentioned|p15|||Geochemistry program||||||
28634|Kanmantoo Group|35744|6|Mentioned|p3|||||||||
28634|Kanmantoo Group|36198|6|Mentioned|p280|||||||||
28634|Kanmantoo Group|36534|6|Mentioned|p221|||||||||
28634|Kanmantoo Group|36731|4|Described|p125|||||||||
28634|Kanmantoo Group|36816|5|Briefly described|Table 1|||See also Fig.2||||||
28634|Kanmantoo Group|36833|6|Mentioned|p21|||||||||
28634|Kanmantoo Group|36836|6|Mentioned|p39|||||||||
28634|Kanmantoo Group|37132|6|Mentioned|p368|||||||||
28634|Kanmantoo Group|37264|6|Mentioned|p91|||||||||
28634|Kanmantoo Group|37461|6|Mentioned|p346|||||||||
28634|Kanmantoo Group|37501|6|Mentioned|p416|||||||||
28634|Kanmantoo Group|37873|6|Mentioned|p1|||||||||
28634|Kanmantoo Group|38004|6|Mentioned|Table 1|||||||||
28634|Kanmantoo Group|38008|6|Mentioned|p3|||||||||
28634|Kanmantoo Group|38068|5|Briefly described|p69|||See also Fig.4.||||||
28634|Kanmantoo Group|38290|4|Described|p20|||||||||
28634|Kanmantoo Group|38660|6|Mentioned|p89|||||||||
28634|Kanmantoo Group|38699|6|Mentioned|p16|||||||||
28634|Kanmantoo Group|38703|6|Mentioned|p131|||||||||
28634|Kanmantoo Group|38704|6|Mentioned|p133|||||||||
28634|Kanmantoo Group|38873|4|Described|Table 2|||||||||
28634|Kanmantoo Group|38927|4|Described|p45|||||||||
28634|Kanmantoo Group|38932|5|Briefly described|p97|||||||||
28634|Kanmantoo Group|39132|6|Mentioned|p189|||||||||
28634|Kanmantoo Group|39331|6|Mentioned|Fig.0-3|||||||||
28634|Kanmantoo Group|39344|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
28634|Kanmantoo Group|39350|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
28634|Kanmantoo Group|39352|6|Mentioned|Map legend|Late Cambrian|Early Cambrian|Early to Late Cambrian||||||
28634|Kanmantoo Group|39489|6|Mentioned|Fig.1|||||||||
28634|Kanmantoo Group|39524|6|Mentioned|Fig.1|||||||||
28634|Kanmantoo Group|39806|6|Mentioned|p207|||||||||
28634|Kanmantoo Group|39842|6|Mentioned|p5|||||||||
28634|Kanmantoo Group|39880|6|Mentioned|p352|||||||||
28634|Kanmantoo Group|39885|6|Mentioned|p434|||||||||
28634|Kanmantoo Group|39909|6|Mentioned|p5|||||||||
28634|Kanmantoo Group|40003|6|Mentioned|p40|||||||||
28634|Kanmantoo Group|40196|4|Described|p1826|||||||||
28634|Kanmantoo Group|40228|6|Mentioned|p38|||||||||
28634|Kanmantoo Group|40442|4|Described|p16|||||||||
28634|Kanmantoo Group|40454|4|Described|p43|||||||||
28634|Kanmantoo Group|40455|5|Briefly described|p67|||||||||
28634|Kanmantoo Group|40500|6|Mentioned|p139|||||||||
28634|Kanmantoo Group|40501|6|Mentioned|p118|||||||||
28634|Kanmantoo Group|40503|4|Described|p107|||||||||
28634|Kanmantoo Group|40695|6|Mentioned|p3|||||||||
28634|Kanmantoo Group|40761|6|Mentioned|p215|||||||||
28634|Kanmantoo Group|40763|4|Described|p206|||||||||
28634|Kanmantoo Group|40852|6|Mentioned|p32|||||||||
28634|Kanmantoo Group|40856|5|Briefly described|p312|||||||||
28634|Kanmantoo Group|41103|6|Mentioned|p261|||||||||
28634|Kanmantoo Group|41253|5|Briefly described|p57|||||||||
28634|Kanmantoo Group|41400|6|Mentioned|p26|||||||||
28634|Kanmantoo Group|41401|6|Mentioned|p32|||||||||
28634|Kanmantoo Group|41478|5|Briefly described|Table 1|||||||||
28634|Kanmantoo Group|41494|6|Mentioned|p31|||||||||
28634|Kanmantoo Group|41526|6|Mentioned|p10|||||||||
28634|Kanmantoo Group|41570|6|Mentioned|p102|||||||||
28634|Kanmantoo Group|41572|6|Mentioned|p5|||||||||
28634|Kanmantoo Group|41594|5|Briefly described|p48|||||||||
28634|Kanmantoo Group|41853|6|Mentioned|Fig.1|||[Originally entered for NT. CEBMar95]||||||
28634|Kanmantoo Group|41947|5|Briefly described|p16|||||||||
28634|Kanmantoo Group|42115|6|Mentioned|p6|||||||||
28634|Kanmantoo Group|42119|5|Briefly described|p523|||||||||
28634|Kanmantoo Group|42129|6|Mentioned|Table 1 P253|||||||||
28634|Kanmantoo Group|42138|6|Mentioned|p388|||||||||
28634|Kanmantoo Group|42154|5|Briefly described|p336|||||||||
28634|Kanmantoo Group|42167|6|Mentioned|Fig.2 P115|||||||||
28634|Kanmantoo Group|42192|6|Mentioned|p4|||||||||
28634|Kanmantoo Group|42222|5|Briefly described|p11|||||||||
28634|Kanmantoo Group|42225|6|Mentioned|Fig.4 P224|||||||||
28634|Kanmantoo Group|42232|6|Mentioned|Fig.1 P269|||||||||
28634|Kanmantoo Group|42242|6|Mentioned|p200|||||||||
28634|Kanmantoo Group|42243|4|Described|p211|||||||||
28634|Kanmantoo Group|42245|6|Mentioned|p37|||[Originally entered for NT. CEBMar95]||||||
28634|Kanmantoo Group|42246|6|Mentioned|p10|||||||||
28634|Kanmantoo Group|42266|5|Briefly described|p291|||||||||
28634|Kanmantoo Group|42268|5|Briefly described|p327|||||||||
28634|Kanmantoo Group|42270|4|Described|p353|||||||||
28634|Kanmantoo Group|42271|6|Mentioned|p369|||||||||
28634|Kanmantoo Group|42272|6|Mentioned|p398|||||||||
28634|Kanmantoo Group|42273|5|Briefly described|p422|||||||||
28634|Kanmantoo Group|42275|6|Mentioned|p465|||||||||
28634|Kanmantoo Group|42276|5|Briefly described|p482|||||||||
28634|Kanmantoo Group|42357|5|Briefly described|p10|||||||||
28634|Kanmantoo Group|42439|6|Mentioned|p351|||||||||
28634|Kanmantoo Group|42487|5|Briefly described|p122|||||||||
28634|Kanmantoo Group|42488|5|Briefly described|Fig.1C P186|||||||||
28634|Kanmantoo Group|42499|5|Briefly described|Map legend|Cambrian||||||||
28634|Kanmantoo Group|42505|5|Briefly described|Map legend|Cambrian||||||||
28634|Kanmantoo Group|42599|5|Briefly described|Fig.3 P614|||||||||
28634|Kanmantoo Group|42601|6|Mentioned|Fig.2 p15|||||||||
28634|Kanmantoo Group|42717|5|Briefly described|map legend|Cambrian||||||||
28634|Kanmantoo Group|42761|5|Briefly described|Fig.1 P6|||||||||
28634|Kanmantoo Group|42788|5|Briefly described|p139, p147|||||||||
28634|Kanmantoo Group|42884|5|Briefly described|p10|||see also Fig.1 p11.||||||17-JAN-07
28634|Kanmantoo Group|42903|5|Briefly described|p424|||see also Fig.1 p423.||||||17-JAN-07
28634|Kanmantoo Group|42966|5|Briefly described|p407|||||||||
28634|Kanmantoo Group|42982|6|Mentioned|Table 1,p333|||||||||
28634|Kanmantoo Group|43027|6|Mentioned|p599|||||||||
28634|Kanmantoo Group|43052|5|Briefly described|p105|||||||||
28634|Kanmantoo Group|43053|5|Briefly described|Map Legend|Cambrian|Cambrian|Marine metasandstone, phyllite, schist, gneiss, minor calcsilicate and marble; pyritic metasiltstone.||||||25-MAY-05
28634|Kanmantoo Group|43073|5|Briefly described|Table 1|||||||||
28634|Kanmantoo Group|43190|5|Briefly described|Fig.1,p28.||Cambrian|see also Fig.2,p29.Age early to ?middle Cambrian.||||||
28634|Kanmantoo Group|43192|6|Mentioned|p58||Cambrian|||||||
28634|Kanmantoo Group|43193|6|Mentioned|p71,78.|||||||||
28634|Kanmantoo Group|43195|5|Briefly described|Map Legend||Cambrian|||||||
28634|Kanmantoo Group|43200|6|Mentioned|p4|||||||||
28634|Kanmantoo Group|43218|4|Described|Fig.3,p22||Cambrian|||||||
28634|Kanmantoo Group|43258|5|Briefly described|Map Legend||Cambrian|||||||
28634|Kanmantoo Group|43298|5|Briefly described|Map Legend||Cambrian|||||||
28634|Kanmantoo Group|43560|6|Mentioned|p234||Cambrian|||||||
28634|Kanmantoo Group|43595|6|Mentioned|p545||Cambrian|||||||
28634|Kanmantoo Group|43627|6|Mentioned|p7|||||||||28-OCT-04
28634|Kanmantoo Group|43660|6|Mentioned|Fig.6,p15||Cambrian|||||||
28634|Kanmantoo Group|43686|5|Briefly described|p235||Cambrian|||||||
28634|Kanmantoo Group|43703|4|Described|p75|||||||||
28634|Kanmantoo Group|43759|4|Described|p445|Middle Cambrian|Early Cambrian|||||||
28634|Kanmantoo Group|43800|5|Briefly described|p169-170|||||||||
28634|Kanmantoo Group|43814|6|Mentioned|Fig.3,p115|||||||||
28634|Kanmantoo Group|44093|6|Mentioned|p47, p108|||Age: Cambrian? Geological Provinve: Kanmantoo Fold Belt.||||||
28634|Kanmantoo Group|44133|5|Briefly described|p6, 14, 17|Cambrian|Cambrian|Metasediments and volcanics.||||||
28634|Kanmantoo Group|44191|6|Mentioned|Map Legend|Middle Cambrian|Early Cambrian|||||||
28634|Kanmantoo Group|48911|6|Mentioned|p7|||Cambrian. Lithology||||||
28634|Kanmantoo Group|48977|6|Mentioned|p19|||Underlies Duntroon Embayment. Under Otway Basin P24. See P56||||||
28634|Kanmantoo Group|49040|6|Mentioned|Plate 1|||||||||
28634|Kanmantoo Group|49060|6|Mentioned|p67|||||||||
28634|Kanmantoo Group|50154|5|Briefly described|p22, p65|Early Cambrian|Early Cambrian|Of Moralana Supergroup. Overlies Normanville Group. Age: 500-600 Ma (detrital zircons). Includes the Karinya Shale. See also the Kanmantoo group.||||||25-AUG-04
28634|Kanmantoo Group|60544|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
28634|Kanmantoo Group|60567|5|Briefly described|p37, p39|||Undifferentiated greywackes of the group now classified as Teal Flat and Marne River Volcanics.||||||
28634|Kanmantoo Group|60712|5|Briefly described|p27, p30 Fig. 3|Early Cambrian|Early Cambrian|Thick succession of metamorphosed mudstone and lithic sandstone. Overlies Normanville Group.  Geological Province: Kanmantoo Trough (Adelaide Geosyncline).  See also p28 Fig. 1.||||||
28634|Kanmantoo Group|60889|6|Mentioned|p249|||Correlation with Billy Creek Formation (Arrowie Basin) and alternative views are presented in text (p249). Stansbury Basin.|||||Clastic dominated, rapidly deposited.|
28634|Kanmantoo Group|60904|5|Briefly described|p803, p804 24a|Early Cambrian|Early Cambrian|Age: ca.532-526Ma.  Of the Lachlan Orogen.||||||17-JAN-07
28634|Kanmantoo Group|60953|5|Briefly described|Map Legend|Cambrian|Cambrian|Marine metasandstone, phyllite, schist, gneiss, minor calcsilicate and marble.||||||
28634|Kanmantoo Group|60958|6|Mentioned|Map Legend|Cambrian|Cambrian|Erratics of this unit in Cape Jervis Formation.||||||
28634|Kanmantoo Group|61046|5|Briefly described|p7|Early Cambrian|Early Cambrian|Includes Tapanappa Formation.||||||
28634|Kanmantoo Group|61108|5|Briefly described|map legend|Cambrian|Cambrian|Marine metasandstone, phyllite, schist, gneiss, minor calcsilicate rock and marble.||||||
28634|Kanmantoo Group|61180|6|Mentioned|p5|||In South Australia.||||||
28634|Kanmantoo Group|61182|6|Mentioned|p49|||Includes metamorphics.||||||
28634|Kanmantoo Group|61307|5|Briefly described|p6 Fig. 3, p7|Middle Cambrian|Early Cambrian|This group has a complex history of stratigraphic nomenclature (details on p7). Geological Province: Adelaide Fold Belt. See also p3-4 Figs. 1 and 2.||||||
28634|Kanmantoo Group|61314|5|Briefly described|p128|Cambrian|Cambrian|Metamorphosed deep water clastic sediments that underlie the Murray Basin. Consist of phyllite, slate and metagreywacke. ||||||
28634|Kanmantoo Group|61411|6|Mentioned|p4 Fig.1.||Cambrian|||||||
28634|Kanmantoo Group|61412|6|Mentioned|p4 Fig.1. ||Cambrian|||||||
28634|Kanmantoo Group|61547|6|Mentioned|p461 Fig.2.|Paleozoic|Paleozoic|Equivalent units underlie the Jurassic and younger rocks of the Penola Trough, Otway Basin.||||||
28634|Kanmantoo Group|61622|6|Mentioned|p436, p440, p436 Fig. 2|Paleozoic|Paleozoic|Geological Province: Otway Basin.||||||07-FEB-11
28634|Kanmantoo Group|61726|5|Briefly described|p925||Early Cambrian|Includes turbidities. Geological Province: Adelaide Fold Belt.||||||
28634|Kanmantoo Group|61752|6|Mentioned|p5|||||||||07-FEB-11
28634|Kanmantoo Group|61762|6|Mentioned|p17|Cambrian|Cambrian|||||||
28634|Kanmantoo Group|61838|5|Briefly described|p221|Cambrian|Cambrian|Includes the Nairne Pyrite Member.||||||
28634|Kanmantoo Group|62742|5|Briefly described|p699 Fig. 2|Early Cambrian|Early Cambrian|||||||
28634|Kanmantoo Group|62744|5|Briefly described|p709 Fig. 2|Early Cambrian|Early Cambrian|||||||
28634|Kanmantoo Group|63020|5|Briefly described|p972 Fig. 1b, p973|Early Cambrian|Early Cambrian|See also p974 Fig. 2. ||||||
28634|Kanmantoo Group|63122|5|Briefly described|p16, p17 Fig. 4.3|Cambrian|Cambrian|Geological Province: Otway Basin. Metasediments and volcanics.||||||
28634|Kanmantoo Group|63124|6|Mentioned|p49, p77|Cambrian|Cambrian|Geological Province: Otway Basin. Mentioned only in terms of equivalents in Figure 5.1.||||||
28634|Kanmantoo Group|63431|5|Briefly described|p677 Fig. 2|Paleozoic|Paleozoic|mentioned in terms of equivalents only.||||||07-FEB-11
28634|Kanmantoo Group|63433|6|Mentioned|p768, p769|||In South Australia. ||||||
28634|Kanmantoo Group|63562|6|Mentioned|p353 Fig.11.||||||Includes Balquhidder Formation.|||
28634|Kanmantoo Group|63599|6|Mentioned|p986|||Geological Province: Adelaide Fold Belt.||||||10-DEC-07
28634|Kanmantoo Group|63793|6|Mentioned|p22.|||Eastern Mount Lofty Ranges. Equivalent to Teltawongee beds in NSW.||||||
28634|Kanmantoo Group|63848|5|Briefly described|p531, p532, p534 Fig.4, p538.|||About 8 km thick, yet deposited within about 12 million years. Fossils are rare, but include trace fossils of Helminthoidichnites and Psammichnites gigas.|||Includes Carrickalinga Head, Talisker, Tapanappa and Tunkalilla  Formations.|||
28634|Kanmantoo Group|64233|5|Briefly described|p22 Fig. 2|Cambrian|Cambrian|Part of a sediments and metasediments group.||||||
28634|Kanmantoo Group|64281|5|Briefly described|p28|Cambrian|Cambrian|Geological Province: Stansbury Basin - where the basinal sequence is locally folded against the Gawler Craton, and against Kangaroo Island Group rocks. . Deep marine terrigenous sediments.||||||23-DEC-09
28634|Kanmantoo Group|64282|6|Mentioned|Map legend|Cambrian|Cambrian|Mentioned in the context of forming pebbles, boulders and residual erratics within the diamictite section of Cape Jervis Formation.||||||
28634|Kanmantoo Group|64334|6|Mentioned|p46|Cambrian|Cambrian|"SE South Australia. Marks the first appearance of the ""Gondwana pattern"" of Late Cambrian to Middle Ordovician zircon age spectrum. Probability density plots."|||||Predominantly turbiditic.|
28634|Kanmantoo Group|64571|6|Mentioned|p835, p836|Early Cambrian|Early Cambrian|Thickness: ~8000m.||||||15-DEC-08
28634|Kanmantoo Group|64647|5|Briefly described|p38, p38 Fig. 1, p39, p44|Cambrian|Cambrian|Overlies Burra Group. Intruded by Rathjen Gneiss. Marnie sediments.||||||
28634|Kanmantoo Group|64705|5|Briefly described|p80 Fig. 7e (photo)|Cambrian|Cambrian|Age: ~520Ma. Metamorphics.||||||04-DEC-08
28634|Kanmantoo Group|64746|6|Mentioned|p394. |||Contains detrital zircons aged 950-900 Ma.|||Includes Carrickalinga Head Formation.|||
28634|Kanmantoo Group|65375|5|Briefly described|p33.|Cambrian|Cambrian||||Includes Carrickalinga Head, Backstairs Passage, Tapanappa, Tunkalilla, Balquhidder and Petrel Cove Formations; Talisker Calc-siltstone; Middleton Sandstone.|Overlies Normanville Group.||
28634|Kanmantoo Group|65376|6|Mentioned|p92 Fig. 2.82. |Cambrian|Cambrian|||||||
28634|Kanmantoo Group|65624|5|Briefly described|map legend|Ordovician|Cambrian|Quartzites, argillaceous schistose quartzites and schistose slates; coarse glaciofluvial conglomerate bands at Penneshaw; ubiquitous slump bedding of Kangaroo Island||||||12-JAN-10
28634|Kanmantoo Group|65664|3|Fully described|pp1095-1108|Early Cambrian|Early Cambrian|Age constrained between underlying Heatherdale Shale and magmatism. 7-8 km thick. Probably laterally equivalent with the Glenelg River Complex.|522 +/- 2 Ma to 514 +/- 3 Ma.||Includes Keynes and Bollaparudda Subgroups.|Overlies Heatherdale Shale (Normanville Group).||09-MAY-12
28634|Kanmantoo Group|65686|5|Briefly described|p408||Cambrian|Stansbury Basin. Includes trilobites.||||Overlies the Heatherdale Shale unconformably.||07-MAY-12
28634|Kanmantoo Group|65892|5|Briefly described|p9 Fig.4, p10, p16, p19.|Middle Cambrian|Early Cambrian|Fleurieu Peninsula. Largely unfossiliferous. Total thickness about 10 km includes two successions separated by an unconformity.|||Includes Carrickalinga Head, Backstairs Passage, Talisker, Tapanappa, Tunkalilla, Balquhidder and Petrel Cove Formations; and Middleton Sandstone.|Overlies Normanton Group.|Two successions of turbidites passing upwards into shallow-water sandstones.|
28634|Kanmantoo Group|65921|5|Briefly described|p1, p2 (map legend).|Cambrian|Cambrian|Deposited in outer shelf, continental slope, and ocean basin environments. Intense deformation and metamorphism, complex fold patterns and melting and granite inclusions are observable. Occurs as inclusions in the Cape Willoughby Granite.|||Carrickalinga Head Formation, Backstairs Passage Formation, Talisker Calcsiltstone, Tapanappa Formation, Tunkalilla Formation, Balquhidder Formation, Petrel Cove Formation, Middleton Sandstone.||Silts and sandstones.|10-JAN-17
28634|Kanmantoo Group|66623|6|Mentioned|p425.|||Correlated in age and facies with Teltawongee Group, Koonenberry Belt.|||Includes basal Carrickalinga Head Formation.|||
28634|Kanmantoo Group|66761|5|Briefly described|p245 Fig.2, p254|Cambrian|Cambrian|Fleurieu Peninsula. Correlated with Minlaton Formation, Yorke Peninsula, and Kangaroo Island Group, in part.||||||
28634|Kanmantoo Group|67103|6|Mentioned|p612, 614-615, 621|||Deposition of these sediments was likely syn-orogenic. The source of zircons in the Rathjen Gneiss. Detrital zircon age spectra.||||||
28634|Kanmantoo Group|67104|6|Mentioned|p629|||||||||
28634|Kanmantoo Group|67536|5|Briefly described|Map Legend|||Kanmantoo Province; basement to Murray Basin.||||Intercalated with Teal Flat Volcanics, Marne River Volcanics, and/or Truro Volcanics|Metasandstone, phyllite, schist, gneiss.|
28634|Kanmantoo Group|68314|5|Briefly described|p749-750, p754-755, p757|Early Cambrian|Early Cambrian|Major influx of foreland siliciclastic detritus in the Delamerian Orogen from c.526 Ma. Similar detrital compositions and depositional characteristics to Leviathan Formation. Has an inferred mid- to late-Early Cambrian age.|||||Quartz-rich turbidites.|
28634|Kanmantoo Group|68315|6|Mentioned|p772-773|Middle Cambrian|Middle Cambrian|Crops out in the southern Delamerian Orogen.||||||
28634|Kanmantoo Group|68731|6|Mentioned|p216, p217|||||||||
28634|Kanmantoo Group|68735|5|Briefly described|p231, p233, p233 Fig.2, p235 Fig.3, p239|Middle Cambrian|Early Cambrian|Stansbury Basin. > 8 km thick. Deposited predominantly below wave base as turbidites, with some shallow water facies. The base of this Group correlates with the bases of both the Billy Creek and Minlaton formations.|||Includes Middleton Sandstone; Petrel Cove, Balquhidder. Tunkalilla, Tapanappa, Talisker, Backstairs Passage, and Carrickalinga Head Formations.|||10-APR-17
28634|Kanmantoo Group|68822|6|Mentioned|p324, p331, p333|Stage 5||Intruded by ca 506 to 490 Ma syntectonic granites.||||||
28634|Kanmantoo Group|68993|5|Briefly described|p544 Fig.1|Middle Cambrian|Early Cambrian||||Middleton Sandstone; Petrel Cove, Balquhidder, Tunkalilla, Tapanappa, Talisker, Backstairs Passage and Carrickalinga Head Formations.|||28-JUL-15
28634|Kanmantoo Group|69213|5|Briefly described|p37, p38, Fig. 14, p24|Early Cambrian||Includes migmatites of Delamerian [Orogeny] age (~500 Ma)|||Includes Carrickalinga Head Formation|Underlain by Neoproterozoic sediments.|Shallow and deep water mainly clastic sediments.|
28634|Kanmantoo Group|69255|5|Briefly described|p770 Fig.1, p771|Cambrian|Cambrian||Between 522-515 Ma.||||Sedimentary rocks and metasediments.|
28634|Kanmantoo Group|69372|6|Mentioned|p27 fig. 5, p30|Cambrian|Cambrian|Forms bedrock in some regions.||||Underlies Cape Jervis Formation|Shows glaciation striations and textures.|
28634|Kanmantoo Group|69562|6|Mentioned|p684|||||||||
28634|Kanmantoo Group|69876|6|Mentioned|p313|||87Sr/86Sr ratios.||||||
28634|Kanmantoo Group|70025|6|Mentioned|p17|||||||||
28634|Kanmantoo Group|70125|5|Briefly described|p399-401, p403 Fig.15|Early Cambrian|Early Cambrian|Haines et al. (2009) rule out Australia as the source of sediments in this unit in favour of a source beneath the East Antarctic ice sheet.||||||
28634|Kanmantoo Group|70382|5|Briefly described|p32-34|Early Cambrian|Early Cambrian|Deformed and metamorphosed during Cambrian Delamarian Orogeny. Over 8km thick turbiditic sequence.|||Includes Carrickalinga Head Formation.|||
28634|Kanmantoo Group|70407|6|Mentioned|p112||Cambrian||||Includes Milendella Limestone.|||
28634|Kanmantoo Group|70493|6|Mentioned|p56, 63|Early Cambrian|Early Cambrian|Delamerian Orogen, SA. East of the Gawler Craton. Considered unlikely as a sediment source for the Adaminaby Group.||||Overlies Normanville Group.||
28634|Kanmantoo Group|70744|5|Briefly described|p935 Fig.2,p936-937,p943-945,p946 Fig.14|Cambrian|Cambrian|SE Delamerian Orogen. Consists of tectonised, mainly deep-marine sedimentary rocks. Up to 8000m thick. Equivalent to NE Thomson Orogen basement. Detrital zircons are of the Pacific-Gondwana (600-510 Ma) signature; age distribution graph.|524-514 Ma (Haines and Flottmann, 1998).||||Siliciclastic turbidites and local shallow-marine sedimentary rocks.|
28634|Kanmantoo Group|70803|5|Briefly described|p5-p7, p11, p42|Early Cambrian|Early Cambrian|Kanmantoo Trough. Deposited in a subsiding basin or marginal shelf setting.|||||Poorly sorted silts including turbidites.|
28634|Kanmantoo Group|70833|5|Briefly described|p200|Cambrian|Cambrian|Of Eastern Stansbury Basin.||||Underlain unconformably by Heatherdale Shale.||
28634|Kanmantoo Group|70838|6|Mentioned|p267 Fig.1, p271, p277|||Possible tectonic settings discussed.||||||
28634|Kanmantoo Group|70840|6|Mentioned|p444|Cambrian|Cambrian|Geological province: Delamerian Orogen. Comparable detrital zircon age spectra to the northern Victoria Land Neoproterozoic-early paleozoic metasedimentary rocks.||||||
28634|Kanmantoo Group|70865|6|Mentioned|p2|||Adelaide Hills area.|||Nairne Pyrite Member.||Fine-grained greywackes, quartzites and siltstones.|
28634|Kanmantoo Group|70877|6|Mentioned|p168|||||||Equivalent to the Glenthompson Sandstone.||
28634|Kanmantoo Group|71139|6|Mentioned|p152-159, 161|||Adelaide Geosyncline. Pb, Th, U concentrations and Pb isotope data tabulated. Often referred to in the article as Kanmantoo sediment.|>526 Ma (Cooper et al., 1992).|||Overlies Normanville Group. Interbedded with Truro Volcanics.||
28634|Kanmantoo Group|71322|5|Briefly described|p52 Fig.1, p73|Cambrian|Cambrian|||||Intrercalated with Truro Volcanics.|Sandstone; siltstone, occasionally sulfidic; metamorphosed.|
28634|Kanmantoo Group|71348|6|Mentioned|p217|||Affected by Delamerian Orogeny. Rift complex that developed at the southern margin of Gondwanan supercontinent.||||||
28634|Kanmantoo Group|71593|4|Described|p19-p22, p26, p121-p123|Early Cambrian|Early Cambrian|MORB-like rocks. See also p126, p150, p166, p169-p171, p180, p195, p198.|c. 510 Ma|Moralana Supergroup|Includes the Tapanappa Formation.|Disconformably overlies the Normanville Group. Overlies the Truro Volcanics and Heatherdale Shale. Equivalent (in part) to the Nangeela Formation.|Basaltic rocks and MORB-like mafic rocks.|
28634|Kanmantoo Group|73059|5|Briefly described|p1059, 1061-1062, 1064|Early Cambrian|Early Cambrian|Delamerian Fold Belt, South Australia. Contains a substantial 700-500 Ma peak of detrital zircons. Formed in a synorogenic basinal setting, not in an extensional basin setting.||||Overlies Normanville Group.||
28634|Kanmantoo Group|73092|6|Mentioned|p2|Cambrian|Neoproterozoic|||||||
28634|Kanmantoo Group|73093|5|Briefly described|map legend|Cambrian|Cambrian|Shown as 3 distinct units. One sedimentary, the others dominantly igneous. Ek and EK?: Marine metasandstone, phyllite, schist, gneiss, minor calcsilicate rock and marble. Ek3?:dolerite/basalt and minor siltstone. Ek4? Basalt-dolerite, minor siltstone, schist; intruded by granite.|||||Marine metasandstone, phyllite, schist, gneiss, minor calcsilicate rock and marble. Dolerite/basalt and siltstone.|12-DEC-21
28634|Kanmantoo Group|73107|5|Briefly described|Map legend.|Early Cambrian|Early Cambrian|Kanmantoo Trough. Several facies are mapped separately.|||Carrickalinga Head, Backstairs Passage, Tapanappa, Tunkalilla, Balquhidder, Petrel Cove Formations; Talisker Calc-Siltstone; Middleton Sandstone.||Undifferentiated: grey metasandstone; migmatised, granitised, mylonitised metasediments. Lithologies detailed in the map legend.|
28634|Kanmantoo Group|73118|6|Mentioned|p8, 15, 21|||||||Correlated with Glenelg Zone in western Victoria.|Metasediments.|
28634|Kanmantoo Group|73129|6|Mentioned|p45|||||||||
28634|Kanmantoo Group|73188|5|Briefly described|p: 310-311, 315-317, 339-344, 349-354|Early Cambrian|Early Cambrian|Mount Lofty Ranges, Kanmantoo Trough. Thrust over Pleistocene alluvial fanglomerate at Saunders Creek by the Cenozoic Milendella Fault. Extremely thick succession; deposited rapidly. Better developed in the eastern and southern Mount Lofty Ranges. Deposition was followed by the Delamerian Orogeny. Type section along the south coast of Fleurieu Peninsula.|||Bollaparudda Subgroup, Keynes Subgroup and units therein|Disconformably underlain by Heatherdale Shale (Normanville Group).|Turbidites and shallow-marine sandstones; variously metamorphosed.|
28634|Kanmantoo Group|73228|6|Mentioned|p50-53|Cambrian|Cambrian|Basement.||||Unconformably overlain by Urana Formation.||
28634|Kanmantoo Group|73229|6|Mentioned|p67|early Paleozoic|Neoproterozoic|Basement.||||||
28634|Kanmantoo Group|73236|6|Mentioned|p47|Cambrian|Cambrian|Fleurieu Peninsula; eroded from the Hallett Cove area.|c. 530-510 Ma||||Turbidite-dominated.|
28634|Kanmantoo Group|73247|6|Mentioned|p205, p210|Cambrian (Stage 4)|Cambrian (Stage 4)|Fleurieu Peninsula.||||Unconformably underlain by Heatherdale Shale. Equivalent to Boxing Bay Formation, Emu Bay Shale, Marsden Sandstone, and White Point Conglomerate.|Includes turbidites.|
28634|Kanmantoo Group|73253|6|Mentioned|p15-16|||Adelaide Fold Belt. Characterised by a main zircon population between 700-500 Ma, with a subordinate population between 1200-900 Ma and scattered older zircon ages of 3500-2000 Ma.|||||Includes metasandstones.|
28634|Kanmantoo Group|73264|6|Mentioned|p1386 Fig.9, p1387 Fig.10, p1388|||Adelaide Rift Complex. Marked by introduction of a Panafrican zircon population (~500-650 Ma) and a smaller Grenvillian population (~900-1200 Ma), probably derived from Antarctica. Correlatives of Kanmantoo Group shown p1386 Fig.9 as Cambrian deep water sediments, Delamerian Supercycle.|||Balquidder Formation, Carrickalinga Head Formation|||
28634|Kanmantoo Group|73430|5|Briefly described|p490-493, p495, p497, p507, p512, p518|Early Cambrian|Early Cambrian|Delamerian Orogen. Rapidly deposited in a deep basin and includes a prominent 550-560 Ma source. Sedimentation terminated by an early D1 fold-thrust phase of deformation, possibly as early as 515 Ma. Ar-Ar muscovite ages of 504.7+/-5.5 Ma, 501+/-4.9 Ma and 501.3+/-18 Ma interpreted as cooling ages, from NW Kangaroo Island. Hosts mafic sills or dykes of tholeiitic composition including the Cape Hart dykes, Woodside dykes. Hosts late syn-tectonic 495+/-1.2 Ma granite intrusions of adakite affinity at Kinchina quarry. Equated with Harvester's Creek greywacke (Gibson et al., 2015). Extends from western Kangaroo Island to the western Victorian Glenelg Terrane (Harvester's Creek greywacke). [See also Kanmantoo group p516-517, Kanmantoo complex and Kanmantoo migmatite complexes p513, Kanmantoo Migmatite p505.]||||Overlies Normanville Group, unconformably underlies Mount Monster rhyolite|Thick-bedded siliciclastic-rich turbidites at base. Includes folded metamorphic complexes; deformed amphibolite facies metasedimentary rocks of interbedded sandstone and mudstone recrystallised to black and white pelite-psamite layers.|
28634|Kanmantoo Group|73594|6|Mentioned|p45 Fig.5.19||||||||Volcanics and metasediments.|
28634|Kanmantoo Group|73635|6|Mentioned|p1, p3, p9|Early Cambrian|Early Cambrian|~9000 m thick in the Kanmantoo Trough. Deformed in the Delamerian Orogeny. Intruded by Cambrian granites.|532-514 Ma||||Sedimentary.|
28634|Kanmantoo Group|74367|5|Briefly described|p6-7, p22|||||||Overlies Normanville Group. Intruded by Rathjen Gneiss|Marine metasandstone, phyllite, schist, gneiss, minor calcsilicat and marble.|
73550|Kara Formation|66623|1|Redefined|pp19-25, p28, pp12-17.|Early Cambrian|Neoproterozoic|Redefined in this publication. Correlative of Farnell Group and by inference Wilpena Group. Has oncolites and possible lenticular stromatolites. Formerly part of Torrowangee Series (Mawson 1912), Wonominta beds (Warris 1967), then Kara beds (Mills 1992). Hosting clear extrusive and intrusive realationship with Mount Arrowsmith Volcanics (p28).||Unit in Grey Range Group.|Includes Gravel Creek Member.|Is overlain by Nundora Formation (Teltawongee Group) with gradational conformable contact. Locally intruded by gabbroic to wehrlitic sills of Mount Arrowsmith Volcanics.|Mustard-coloured, intercalated dolomite, quartzite, limestone, siltstone, sandstone units; metamorphosed to greenschist facies. Shows bedding, cross-bedding, ripple marks and laminations.|24-SEP-13
73550|Kara Formation|66917|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Several un-named units are mapped separately.||Unit in Grey Range Group.|Includes Gravel Creek Member.|Overlies Mount Arrowsmith Volcanics.|Variably cleaved phyllite and minor quartzite; interbedded sandstone and siltstone with minor dolomitic and calcareous beds; ripples, bioturbation, cross-bedding and load structures; regionally metamorphosed to greenschist facies.|
73550|Kara Formation|66918|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Four un-named units are mapped separately.||Unit in Grey Range Group.|||Variably cleaved phyllite and minor quartzite; interbedded sandstone and siltstone with minor dolomitic and calcareous beds; ripples, bioturbation, cross-bedding and load structures; regionally metamorphosed to greenschist facies.|
73550|Kara Formation|66927|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Zones of low magnetic intensity with local narrow trends of moderate magnetic intensity which may relate to narrow mafic sills and flows.||||Overlies Mount Arrowsmith Volcanics.|Phyllite, quartzite, sandstone and siltstone; minor dolomitic and calcareous beds.|
73550|Kara Formation|67105|5|Briefly described|p654- 655, 659, 661|Ediacaran|Ediacaran|Wonnaminta Zone, Koonenberry Belt.||Grey Range Group.||Is overlain (probably disconformably) locally by the Nundora Formation.|Shallow-marine sedimentary rocks.|
73550|Kara Formation|67207|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|||Unit in Grey Range Group.|||Variably cleaved phyllite and minor quartzite; interbedded sandstone and siltstone with minor dolomitic and calcareous beds; ripples, bioturbation, cross-bedding; massive yellow, dolomitised limestone with variable lithic component.|
73550|Kara Formation|67208|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Seven un-named sub-units with differing lithologies are mapped separately.||Lower unit in Grey Range Group|Includes basal Gravel Creek Member.||Variably cleaved phyllite and minor quartzite; interbedded sandstone and siltstone with minor dolomitic and calcareous beds; oolitic limestones, quartzite, quartzose sandstones, minor basaltic volcanics.|
73550|Kara Formation|67211|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|||Unit in Grey Range Group.|||Variably cleaved phyllite and minor quartzite; interbedded sandstone and siltstone with minor dolomitic and calcareous beds; ripples, bioturbation, cross-bedding and load structures; regionally metamorphosed to greenschist facies.|
73550|Kara Formation|67322|5|Briefly described|p9|Neoproterozoic|Neoproterozoic|W flank of Mount Arrowsmith, northern end of the Koonenberry Belt.||||Overlain by the Pincally Formation.||22-FEB-18
73550|Kara Formation|69961|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|||Unit in Grey Range Group.|||Variably cleaved phyllite and minor quartzite; interbedded sandstone and siltstone with minor dolomitic and calcareous beds; ripples, bioturbation, cross-bedding and load structures; regionally metamorphosed to greenschist facies.|
73550|Kara Formation|70648|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|3 un-named units: Metasedimentary sequence dominated by metre-scale thick quartzite horizons; originally quartz-rich sandstone. Pink to grey limestone with variable lithic component; regionally metamorphosed to lower greenschist facies. Dark grey to green cryptocrystalline chert with discontinuous boudinaged lenses up to 2m thick.||Grey Range Group|Includes 3 un-named units.||Variably cleaved phyllite and minor quartzite; interbedded sandstone and siltstone with minor dolomitic and calcareous beds; ripples, bioturbation, cross-bedding and load structures; regionally metamorphosed to greenschist facies.|
73550|Kara Formation|70650|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|4 unnamed units: multiply deformed biotite-muscovite schist; originally interbedded mudstone and sandstone, with minor feldspathic sandstone, quartz-hematite-magnetite and dolomitic limestone lenses; regionally metamorphosed to lower amphibolite facies. Metasedimentary sequence dominated by metre scale thick quartzite horizons; originally quartz-rich sandstone; regionally metamorphosed to greenschist facies. Pink to grey limestone with variable lithic component; regionally metamorphosed to lower greenschist facies. Buff to red-brown, medium- to coarse-grained lithic-feldspathic sandstone; lithic clasts are mainly volcanic and are poorly-sorted and subangular; regionally metamorphosed to greenschist facies.||Grey Range Group|Includes 4 un-named units.||Variably cleaved phyllite and minor quartzite; interbedded sandstone and siltstone with minor dolomitic and calcareous beds; ripples, bioturbation, cross-bedding and load structures; regionally metamorphosed to greenschist facies.|
73550|Kara Formation|70651|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Unnamed sub-unit is a metasedimentary sequence dominated by metre-scale quartzite horizons; originally quartz-rich sandstone.||Grey Range Group|Includes unnamed sub-unit.||Variably cleaved phyllite and minor quartzite; interbedded sandstone and siltstone with minor dolomitic and calcareous beds; ripples, bioturbation, cross-bedding and load structures; regionally metamorphosed to greenschist facies.|
73550|Kara Formation|70838|4|Described|p268-272, p274-278, p280-281|Ediacaran|Ediacaran|Coeval with Mount Arrowsmith Volcanics. SHRIMP U-Pb zircon age from interbedded rhyolite. Detrital zircon analyses: exclusively Mesoproterozoic source. Provenance discussed: Musgrave Province preferred.|585 +/- 3.2 Ma (Black, 2007).|Grey Range Group.||Is overlain conformably by Nundora Formation (Teltawongee Group).|Finely laminated siltstone and sandstone with  minor chert and limestone.|
73550|Kara Formation|71262|6|Mentioned|p3, p5 Fig 2, p8 Fig 5, p9, p12|Neoproterozoic|Neoproterozoic|||||||
73550|Kara Formation|73093|5|Briefly described|map legend|Neoproterozoic|Neoproterozoic|[the basaltic metavolcanics included in this SA description may be Mount Arrowsmith Volcanics, or equivalent]|||||Phyllite, schist with metasandstone, meta-limestone and basaltic metavolcanics.|12-DEC-21
73550|Kara Formation|73177|5|Briefly described|p1113-1115 Figs.15-17|Neoproterozoic|Neoproterozoic|Delamerian Orogen. Proposed continental rift setting. An MDA of >900 Ma (Johnson et al., 2016) is also given.|585 +/- 3.2 Ma.|Grey Range Group.||||
73550|Kara Formation|74367|6|Mentioned|p16, p18|Cambrian|Neoproterozoic|||Grey Range Group||||
34370|Karinya Shale|22643|5|Briefly described|p191,fig6|Early Cambrian|Early Cambrian|||||||
34370|Karinya Shale|24465|6|Mentioned|p347|Early Cambrian|Early Cambrian|See also "Karinya Shale".||||||
34370|Karinya Shale|44133|5|Briefly described|p4 Fig. 7.2, 16|Early Cambrian|Early Cambrian|Geological Province: Stansbury Basin. Maximum Thickness: 200m. Overlain by: Tapanappa Formation.||||||
34370|Karinya Shale|50154|5|Briefly described|p52|||Of the Kanmantoo Group. Geological Province: Stansbury Basin.||||||
34370|Karinya Shale|60712|4|Described|p34, p28 Fig. 1|Early Cambrian|Early Cambrian|Of Silverton Subgroup (Kanmantoo Gp). Supersedes Karinya Shale Mbr (of the former Brukunga Fm). Black carbonaceous shale; grades upwards into the Tapanappa Fm; overlies Backstairs Passage Fm.  Pebbly sandstone at its base is the Malabena Sst Member.||||||
34370|Karinya Shale|60953|5|Briefly described|Map Legend|Cambrian|Cambrian|Pyritic and carbonaceous metasiltstone.||||||
34370|Karinya Shale|61108|5|Briefly described|map legend|Cambrian|Cambrian|Pyritic and carbonaceous metasiltstone.||||||06-JUN-05
34370|Karinya Shale|61307|5|Briefly described|p6 Fig. 3, p7|Cambrian|Cambrian|Of the Kanmantoo Group. Overlies Backstairs Passage Formation. Geological Province: Karinya Syncline/Adelaide Fold Belt..||||||27-MAY-08
34370|Karinya Shale|73093|5|Briefly described|map legend|Cambrian|Cambrian||||||Shale, siltstone, blue-black, pyritic, laminated, carbonaceous.|09-DEC-21
29269|Karkulta Rhyolite|24474|4|Described|p40|||Of the Glyde Hill Volcanic Complex.  Porphyritic rhyolite, flow-banded rhyolite and rhyolite breccia.  Conformably overlies the Mangaroongah Dacite.  Geological Province: Gawler Craton.||||||
29269|Karkulta Rhyolite|30984|2|Defined|p14|Proterozoic|Proterozoic|||||||
29269|Karkulta Rhyolite|41974|6|Mentioned|Fig.1 P408|||||||||
29269|Karkulta Rhyolite|42468|6|Mentioned|p5|||||||||
29269|Karkulta Rhyolite|43052|5|Briefly described|p111|||of Glyde Hill Volcanic Complex||||||
29269|Karkulta Rhyolite|43071|6|Mentioned|p14|||||||||
29269|Karkulta Rhyolite|69649|5|Briefly described|p20-21|||||Unit in Glyde Hill Volcanic Complex.||Conformably overlies Mangarooongah Dacite.|A small outcrop of porphyritic rhyolite, flow-banded rhyolite and rhyolitic autoclastic breccia. Contains biotite associated with plagioclase phenocrysts.|
29269|Karkulta Rhyolite|70659|5|Briefly described|p7-8|Mesoproterozoic|Mesoproterozoic|||Glyde Hill Volcanic Complex.|||Localised felsic lava flow with coherent core and autobrecciated margins; close to source vent.|
29269|Karkulta Rhyolite|70816|5|Briefly described|p5|||Lake Everard area, Gawler Ranges.||Unit of Glyde Hill Volcanic Complex.||Overlain by, and laterally equivalent to Arburee Rhyolite. Underlain by Mangaroongah Dacite.||
29269|Karkulta Rhyolite|72090|6|Mentioned|p12|||Gawler Craton.||Glyde Hill Volcanic Complex||||
22070|Karlaya Limestone|22746|4|Described|Fig.3 p515, p521|Neoproterozoic III|Neoproterozoic III|See also p523, p528||||||
22070|Karlaya Limestone|22802|6|Mentioned|p872|||Officer Basin||||||
22070|Karlaya Limestone|22922|5|Briefly described|34|||Parent Ungoolya Group||||||
22070|Karlaya Limestone|23282|1|Redefined|p60||Neoproterozoic|Informally introduced by Sukanata (1993) and formally defined as a member of Tanana Formation by Zang (1995). Now raised to formation status. Age: Precambrian, Neoproterozoic, mid Marinoan Epoch. of Ungoolya Gp.||||||
22070|Karlaya Limestone|23524|5|Briefly described|p221 Fig. 3|Neoproterozoic|Neoproterozoic|||||||
22070|Karlaya Limestone|24112|5|Briefly described|p254 Fig.2|Neoproterozoic|Neoproterozoic|Of the Ungoolya Group. Geological Province: Officer Basin||||||
22070|Karlaya Limestone|43743|6|Mentioned|Fig.2,p33||Neoproterozoic|||||||
22070|Karlaya Limestone|50127|6|Mentioned|p48 Fig.2|||Geological Province: Officer Basin||||||
22070|Karlaya Limestone|60565|6|Mentioned|p18|Neoproterozoic|Neoproterozoic|Carbonates||||||
22070|Karlaya Limestone|61732|3|Fully described|p5 Tb. 1, p62|Cryogenian|Cryogenian|Of the Ungoolya Gp. Initially a member of the Tanana Formation. Conformably overlies Dey Dey Mudst; unconformably overlain by Tanana Fm. Max. thickness: ~60m. Geological Prov: Officer Basin. See also p58 Fig. 22, p145 Fig. 51.||||||07-FEB-11
22070|Karlaya Limestone|62453|6|Mentioned|p14|||||||||
22070|Karlaya Limestone|63811|5|Briefly described|p500, 502, 505, Fig 2|Ediacaran|Ediacaran|13 m thick in the Giles 1 (Officer Basin), but known to be up to 66 m thick (in type section).||Of the Ungoolya Group.||Overlies Dey Dey Mudstone. Overlain by Tanana Formation.|Thin bedded micritic limestone with dark grey silty mudstone layers and some limestone intraclasts.|28-MAR-12
22070|Karlaya Limestone|64794|4|Described|p238 fig 2, p241 Tb.1, p242 fig 3, p245|Ediacaran|Ediacaran|See also p247-248, p251-8, p272-273. 61m thick.||Ungoolya Group||Conformably overlies Dey Dey Mudstone. Overlain conformably by Tanana Formation.|Middle 0.5m thick intraclastic calcirudite above 23.3m thick lower micritic limestone with common thin grey shale or marl interbeds, and below 37.2m thick micritic limestone with grey shale interbeds with gradational contacts.|
22070|Karlaya Limestone|64797|6|Mentioned|p153 Fig.2|Ediacaran|Ediacaran|Officer Basin. Lithology/rank not shown on diagram.||||||
22070|Karlaya Limestone|66569|5|Briefly described|p861 fig.2,|Ediacaran|Ediacaran|Of Ungoolya Group; underlies Tanana Formation; unconformably overlies Dey Dey Mudstone.||||||
22070|Karlaya Limestone|67912|5|Briefly described|p12-14, 16|Ediacaran|Ediacaran|Officer Basin. Acanthomorphic acritarchs occur in Lake Maurice West 1 drillhole. The unit is 27.7m thick in the drill core but varies across the Murnaroo Platform. Subtidal shelf environment. Lithostratigraphic column with taxa and revised biozones. Numerous photomicrographs.||Ungoolya Group.||Conformably and transitionally overlies Dey Dey Mudstone. Is overlain by Wilari Dolomite Member (Tanana Formation).|Predominantly thin-bedded micritic limestone with thin dark-grey, silty, mudstone interbeds.|
22070|Karlaya Limestone|67921|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Shown only in section and grouped with Punkerri Sandstone, Ungoolya Group (Rodda beds), Wright Hill beds. Group description: Marine sandstone, grey indurated mudstone and limestone.||Ungoolya Group||Said to be equivalent to Wilpena Group||
22070|Karlaya Limestone|68269|6|Mentioned|p674|Ediacaran|Ediacaran|Officer Basin.||Ungoolya Group||Unconformably underlain by Dey Dey Mudstone. Overlain by Tanana Formation.|Limestone dominated.|
22070|Karlaya Limestone|68271|5|Briefly described|p697|||Officer Basin. Misspelt as Kalaya on p697. Correlative to/overlap in stratigraphic time with Wearing Dolomite Member (Adelaide Rift Complex).||||||
22070|Karlaya Limestone|72478|6|Mentioned|p8|Marinoan|Marinoan|Officer Basin.|c. 590 Ma-585 Ma|Ungoolya Group||Overlies the Dey Dey Mudstone. Underlies the Tanana Formation.||24-MAR-21
22070|Karlaya Limestone|73099|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Officer Basin.||Ungoolya Group.||Overlies Dey Dey Mudstone. Is overlain by Tanana Formation.|Pale to medium grey micritic limestone, thinly interbedded with dark grey, calcareous, silty mudstone.|
22070|Karlaya Limestone|73100|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Subsurface.||||Equivalent to Wilpena Group.||
22070|Karlaya Limestone|73109|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Subsurface.||Ungoolya Group.||||
22070|Karlaya Limestone|73111|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Subsurface.||Ungoolya Group.||||
23690|Katunga Dolomite|22629|6|Mentioned|p149|Paleoproterozoic|Paleoproterozoic|Part of Hutchison Group (Middleback Subgroup).||||||07-NOV-08
23690|Katunga Dolomite|23285|5|Briefly described|Fig 3 p 333|||||||||
23690|Katunga Dolomite|23719|4|Described|p14|Paleoproterozoic|Paleoproterozoic|See also page 14 Table 1. Replaces Middleback North Dolomite. Of Middleback Subgroup. Overlain by Lower Middleback Jaspilite. Underlying unit Warrow Quarzite.  Geological Province: Gawler Craton. Max. Thickness 20 m.||||||23-JUN-09
23690|Katunga Dolomite|23731|5|Briefly described|p20, p27|||Banded, off-white and green marble. Overlain by Lower Middleback Jaspellite.||||||27-MAY-08
23690|Katunga Dolomite|37811|2|Defined|p237|Paleoproterozoic|Paleoproterozoic|Previously "Middleback North Dolomite".||||||07-NOV-08
23690|Katunga Dolomite|39345|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
23690|Katunga Dolomite|39349|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
23690|Katunga Dolomite|39353|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
23690|Katunga Dolomite|39844|6|Mentioned|p60|||||||||
23690|Katunga Dolomite|40227|6|Mentioned|p44|||||||||
23690|Katunga Dolomite|40445|5|Briefly described|p47|||||||||
23690|Katunga Dolomite|40448|6|Mentioned|p30|||||||||
23690|Katunga Dolomite|41619|6|Mentioned|Map legend|Paleoproterozoic||||||||07-NOV-08
23690|Katunga Dolomite|41667|6|Mentioned|p5|||||||||
23690|Katunga Dolomite|42738|5|Briefly described|map legend|Paleoproterozoic||||||||07-NOV-08
23690|Katunga Dolomite|43052|5|Briefly described|p54|||Of Middleback Subgroup.||||||27-MAY-08
23690|Katunga Dolomite|61070|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Middleback Subgroup. Medium-grained, white-grey, massive to compositionally banded dolomite marble. Porphyroblasts of olivine +/- replacement serpentine common. Geological Province: Gawler Craton.||||||12-JAN-10
23690|Katunga Dolomite|61307|5|Briefly described|p37, p61 Fig. 27|Paleoproterozoic|Paleoproterozoic|Of the Hutchison Group. Massive to poorly latered medium-grained dolomitic marbles.  This unit fines upwards into the Middleback Subgroup. Geological Province: Gawler Craton.||||||07-NOV-08
23690|Katunga Dolomite|62893|4|Described|Map Legend, p10, p38-39|Early Proterozoic|Early Proterozoic|Varies greatly in thickness. Comprises a series of metamorphosed shallow-water marine carbonate and marl beds.||Middleback Subgroup, Hutchison Group||Underlain by Warrow Quartzite. Overlain by and interfingers with Lower Middleback Jaspilite.|Massive grey, pink and white dolomitic marble and local interbands of calc-silicate and chert gneiss; occasionally silicified and altered to opalite.|
23690|Katunga Dolomite|65221|5|Briefly described|p27, p28 Fig.3, p30 Fig.5c|Palaeoproterozoic|Palaeoproterozoic|member of the Hutchison Group||||||
23690|Katunga Dolomite|65376|6|Mentioned|p54. |Paleoproterozoic|Paleoproterozoic|||Unit in Middleback Subgroup.||||
23690|Katunga Dolomite|65379|5|Briefly described|p641-642, p643, p644, p648|Paleoproterozoic|Paleoproterozoic|Base of Hutchison Group (Middleback Subgroup). Massive to poorly layered dolomitic marble.  Grades into the overlying lower Middleback Jaspilite. N.B Chrysotile asbestos occurrence and mine host. Contains Cowell and Tumby Bay Asbestos Mines.||||||
23690|Katunga Dolomite|65922|5|Briefly described|p14 Tb. 1, p15, p38|Orosirian|Orosirian|Gawler Craton. Base unit of Middleback Subgroup, Hutchison Group. Interlayered up-sequence with Lower Middleback Jaspilite. Conformably overlies Warrow Quartzite. At the base: ankeritic dolomite marble with local interbands of graphitic schist; middle: biotite-sillimanite-garnet schist and amphibolite; at the top: calcite marble.||||||
23690|Katunga Dolomite|66302|6|Mentioned|p24|||||Hutchison Group||||
23690|Katunga Dolomite|66882|5|Briefly described|p101, p103 Fig.3a,c, p107, p109-114|||Type section in Middleback Range. Dolomitic outcrops formerly mapped under this name in the Lincoln-Cleve uplands (west of the Kalinjala Mylonite Zone) are now part of Poolalalie Dolomite. Isotope data. Geochemistry discussed.||Middleback Group||Underlies Lower Middleback Jaspilite.||
23690|Katunga Dolomite|67323|6|Mentioned|Eastern Australia Time-Space Plot|||Southern Gawler Craton.||||||
23690|Katunga Dolomite|67721|5|Briefly described|p33, p34, p35, p36 Fig.6, p38 Fig.9|Archean|Archean|Type locality defined by Miles (1954) and Parker and Lemon (1982) as 5km SW of Iron Baron, on the western bank of the Middleback Range (WGS84, zone 53, 0700239mE, 6340931mN).||Of the Middleback Group.|||Dolomite.|
23690|Katunga Dolomite|68131|5|Briefly described|p57-58|Paleoproterozoic|Paleoproterozoic|Eastern Eyre Peninsula.||Middleback Subgroup.|||Dolomite.|
23690|Katunga Dolomite|68158|6|Mentioned|p4|||||Hutchison Group.||||
23690|Katunga Dolomite|70659|6|Mentioned|p10|Palaeoproterozoic|Palaeoproterozoic|||||||
23690|Katunga Dolomite|70816|6|Mentioned|p3|Paleoproterozoic|Paleoproterozoic|Gawler Ranges region.||||||19-JUN-19
23690|Katunga Dolomite|70948|6|Mentioned|p974|Paleoproterozoic|Paleoproterozoic|Geological province: Gawler Craton.||||||
23690|Katunga Dolomite|71235|6|Mentioned|p3, p9|Palaeoproterozoic|Palaeoproterozoic|||Hutchison Group||||
23690|Katunga Dolomite|71322|6|Mentioned|p103|Paleoproterozoic|Paleoproterozoic|Northern Eyre Peninsula.||||||
23690|Katunga Dolomite|71418|5|Briefly described|p20|Paleoproterozoic|Paleoproterozoic|Geological province: Gawler Craton.||Unit of Hutchison Group.||||
23690|Katunga Dolomite|71536|5|Briefly described|p79, p88|||Wilgerup sequence.||||Conformably (transitionally) overlain by the Lower Middleback Jaspilite.|Various dolomitic marbles, hematite-siderite marbles and other (meta)carbonate rocks.|
23690|Katunga Dolomite|71859|6|Mentioned|p18|||||Hutchison Group||||
23690|Katunga Dolomite|72058|5|Briefly described|p172|||Middleback Ranges, Gawler Craton.||Middleback Group||Conformably/gradationally overlies the Warrow Quartzite. Overlain by the Lower Middleback Iron Formation.||15-MAR-21
23690|Katunga Dolomite|72464|6|Mentioned|p3|||||||||
23690|Katunga Dolomite|72484|5|Briefly described|p2|||||Middleback Subgroup.||Gradationally overlies Warrow Quartzite. Is overlain gradationally by Lower Middleback Iron Formation.||
23690|Katunga Dolomite|73103|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic||||||Marble, white to pale grey, dolomitic, layered with serpentine, with calcite-diopside-tremolite banding.|
23690|Katunga Dolomite|73110|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|||Middleback Subgroup.|||Marble, white to pale grey, dolomitic, layered with serpentine, with calcite-diopside-tremolite banding.|
23690|Katunga Dolomite|73122|6|Mentioned|p32|||||||Overlies Warrow Quartzite.||
27643|Kenella Gneiss|22613|4|Described|p11|||||||||
27643|Kenella Gneiss|22614|5|Briefly described|map|||||||||
27643|Kenella Gneiss|22629|6|Mentioned|p160|Archean|Archean|||||||07-NOV-08
27643|Kenella Gneiss|24472|5|Briefly described|p5 Tb.1|Archean|Archean|Geological Province: Harris Greenstone Domain, Gawler Craton. Age: 2420 Ma (monazite). Part of the Mulgathing Complex.||||||02-JUN-09
27643|Kenella Gneiss|24505|5|Briefly described|p8|Archean|Archean|Of the Mulgathing Complex.  Hosts vein quartz mineralisation.  Geological Province: Gawler Craton.||||||07-NOV-08
27643|Kenella Gneiss|39802|6|Mentioned|Map legend|Archean|Archean|||||||07-NOV-08
27643|Kenella Gneiss|39905|6|Mentioned|Fig.4|||||||||
27643|Kenella Gneiss|40644|6|Mentioned|p124 Fig. 3,  p126|Paleoproterozoic|Archean|Included in the Mulgathing Complex. Age: 2488+/-130Ma.||||||07-NOV-08
27643|Kenella Gneiss|42465|5|Briefly described|Map Legend|||||||||
27643|Kenella Gneiss|42469|3|Fully described|p10|||||||||
27643|Kenella Gneiss|43052|4|Described|p42,Table 3.2|||Of Mulgathing Complex.||||||02-JUN-09
27643|Kenella Gneiss|44695|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
27643|Kenella Gneiss|44935|5|Briefly described|Map Legend||Proterozoic|||||||
27643|Kenella Gneiss|50605|5|Briefly described|p8.7, 8.10|Archean|Archean|Of the Mulgathering Complex. Geological Province: Gawler Craton and Curnamona Province.||||||02-JUN-09
27643|Kenella Gneiss|60704|6|Mentioned|p685|Archean|Archean|Of the Mulgathing Complex. Geological Province: Gawler Craton.||||||07-NOV-08
27643|Kenella Gneiss|64137|5|Briefly described|p1543|Archean|Archean|Hosts the Earea Dam and South Lake gold occurrences in the Harris Greenstone domain. Neodymium isotope data.||Unit in Mulgathing Complex.||||
27643|Kenella Gneiss|65376|5|Briefly described|pp190-193.||||Protolith age 2509 +/- 3 Ma.|Unit in Mulgathing Complex.|||Mainly acid volcanics.|
27643|Kenella Gneiss|65390|5|Briefly described|p14, p22 Fig. 3|Archean|Archean|Of Mulgathing Complex, Gawler Craton. Felsic extrusives and/or intrusives. Age >2440 Ma. Syn-tectonic with Glenloth Granite.||||||
27643|Kenella Gneiss|66302|5|Briefly described|p10, p11, p61, p61 Fig.14|Neoarchean|Neoarchean|Protolith interpreted to have been deposited between 2535 and 2500 Ma in shallow to moderate depth marine environment in an extensional back arc setting. Interpreted maximum depositional age. |ca. 2535 Ma|Mulgathing Complex|||Massive to layered, K-feldspar-plagioclase-quartz gneiss.|
27643|Kenella Gneiss|66520|6|Mentioned|p10.|||Includes volcaniclastic rocks.|c.2560 Ma zircon age.|||||
27643|Kenella Gneiss|67058|5|Briefly described|p479 Fig. 3|Archean|Archean|See also Kenella Paragneiss p476, 492.|||||paragneiss|07-AUG-15
27643|Kenella Gneiss|67721|6|Mentioned|p35 Fig.5|||||||||
27643|Kenella Gneiss|68128|5|Briefly described|p2-p3, p6, p53, p58|Palaeoproterozoic|Archaean|Gawler Craton. Deposited in a shallow to moderate water depth environment interpreted to have been a restricted, actively subsiding basin. Additional SHRIMP ages include 2474 +/- 4 Ma and 2487 +/- 16 ma (the latter derived from Swain et al, 2005).|2502 +/- 8 Ma (SHRIMP U-Pb)|Mulgathing Complex|||Sedimentary rocks including quartzite, pelite and aluminous pelitic rock in addition to banded iron formations and interlayered carbonates; bimodal volcanic rocks.|
27643|Kenella Gneiss|68131|6|Mentioned|p77|Paleoproterozoic|Archean|||||||
27643|Kenella Gneiss|68208|6|Mentioned|p31 Fig.2|Paleoproterozoic|Neoarchean|||Of Mulgathing Complex||||
27643|Kenella Gneiss|69203|6|Mentioned|p36 Fig.22B|||||||||
27643|Kenella Gneiss|69649|5|Briefly described|p35|Archean|Archean|Harris Greenstone Domain.|||||Felsic extrusives and/or intrusives.|
27643|Kenella Gneiss|70789|5|Briefly described|p316, p320-321|||Part of the crystalline basement to the Gawler Craton. Apatite Fission Track results tabulated; central ages from 354 +/- 17 Ma to 386 +/- 17 Ma indicate exhumation in Devonian - Carboniferous [The depositional/crystallisation age is not discussed].||Mulgathing Complex.|||Metavolcanics.|17-SEP-18
27643|Kenella Gneiss|71536|4|Described|p141-p144, p218|Siderian|Siderian|SHRIMP U-Pb dates are interpreted as the age of magmatic crystallisation. Metamorphism has been dated at 2426 +/- 5 Ma by SHRIMP (this volume). Relationship with other units in the Mulgathing Complex are uncertain. Petrography, zircon characteristics and geochronology results are discussed for two granite samples of this suite.|2468 +/- 5 Ma (SHRIMP U-Pb)|Mulgathing Complex|||Medium- to coarse-grained quartz-K-feldspar dominant, poorly banded  syeno-granite gneiss.|
27643|Kenella Gneiss|71859|5|Briefly described|p2, p28|||Central-western Gawler Craton. Referred to as the Kenella Paragneiss on p28.||Mulgathing Complex.|||Felsic metavolcanic rocks.|
27643|Kenella Gneiss|73230|4|Described|p6-8, p11-12, p15|Siderian|Neoarchean|Gawler Craton. Domain: Harris Greenstone and Wilgena. Hosts gold mineralisation in quartz veins, which is thought to be related to Hiltaba Suite or Gawler Range Volcanics magmatism. Metamorphism at c. 2475-2390 Ma. Interlayered with greenstones of Lake Harris Komatiite, Hopeful Hill Basalt, and South Lake Gabbro. Also intruded by younger unnamed granitoids (c. 2460 Ma). Generally interpreted as a predominantly volcanic and volcaniclastic unit, but could alternatively be a massive, source proximal, quartz-rich sediment. [Lithological] distinction from Christie Gneiss may be somewhat unclear.|c. 2520-2470 Ma (magmatic)|Mulgathing Complex||Intruded by Glenloth Granite.|Orange-pink to reddish-pink volcanic to volcaniclastic gneiss with weak compositional zoning. Minor banded iron formation, calc-silicate rock and metasediment.|
27643|Kenella Gneiss|73235|6|Mentioned|p61, p63|||Hosts gold mineralisation in the Tarcoola and Labyrinth mineral fields of the Kararan (Gawler Range Volcanics) gold mineral system, and in the Western Gawler mineral field of the Kararan (Hiltaba Suite) gold mineral system.||||||
23695|Ketchowla Siltstone|22510|5|Briefly described|p40,table1|||Age: Marinoan||||||
23695|Ketchowla Siltstone|42542|2|Defined|p8|Neoproterozoic||Name reserved.||||||
23695|Ketchowla Siltstone|43052|5|Briefly described|p192,Table 6.1|||Of the Yerelina Subgroup (Umberatana Group).||||||14-MAY-07
23695|Ketchowla Siltstone|61238|4|Described|p46 Fig. 2, p47 Fig. 3|Neoproterozoic|Neoproterozoic|Of the Umberatana Group. Siltstone, calcareous, laminated, scattered quartz granules, isolated dropstones.||||||14-MAY-07
23695|Ketchowla Siltstone|61732|5|Briefly described|p28 Fig. 13|Marinoan|Marinoan|Of the Yerelina Subgroup (Umberatana Group). Geological Province: Adelaide Rift Complex.||||||07-FEB-11
23695|Ketchowla Siltstone|69019|5|Briefly described|p51-52. |Neoproterozoic|Neoproterozoic|Of Preiss (1992). Thickness >110 m.||Unit in Yerelina Subgroup.||Conformably overlies Balparana Sandstone.|Grey and grey-green calcareous siltstone, weathering brownish, laminated, well-bedded; isolated quartzite dropstones.|
23695|Ketchowla Siltstone|72456|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Marree 1:250k map sheet. |||||Siltstone, grey and grey-green siltstone, calcareous, laminated, scattered quartz granules, isolated dropstones.|
23695|Ketchowla Siltstone|73093|5|Briefly described|map legend|Neoproterozoic|Neoproterozoic||||||Siltstone, grey and grey-green, calcareous, laminated, scattered quartz granules, isolated dropstones.|09-DEC-21
22091|Keynes Subgroup|24465|2|Defined|p358, p363 App. 1|Early Cambrian|Early Cambrian|Lower subgroup of the Kanmatoo Group.  Includes Carrickalinga Head Formation and Backstairs Passage Formation.||||||27-OCT-04
22091|Keynes Subgroup|65664|5|Briefly described|p1096, p1106 Fig.5|Early Cambrian|Early Cambrian|||Lower Subgroup of Kanmantoo Group.|Includes Backstairs Passage and Carrickalinga Head Formations.|Unconformably overlies Normanville Group. Unconformably overlain by Bollaparudda Subgroup.||09-MAY-12
22091|Keynes Subgroup|73188|5|Briefly described|p316, p343|Early Cambrian|Early Cambrian|Mount Lofty Ranges.||Kanmantoo Group|Backstairs Passage Formation, Carrickalinga Head Formation|||
37212|Khasta Formation|24396|4|Described|p218 Fi.3, p221|Late Eocene|Late Eocene|See also p220 Fig.4. Estuarine sands with siliceous sponge spicule.  Underlying unit: Pidinga Formation.  Geological Province: Gawler Craton.||||||
37212|Khasta Formation|24397|4|Described|p241|||Replaces Khasta Member of Hampton Sandstone.  Also includes some rocks previously included in the Bring Member of the Pidinga Formation.  Direct equivalent of Pallinup Fm. in WA.  Geological Province: Eucla Basin.||||||
37212|Khasta Formation|24606|4|Described|p957 Fig. 2|Late Eocene|Late Eocene|Overlain by the Upper Ooldea Sand. Overlies the upper Pidinga Formation. Geological Province: Eucla Basin. Formation is Fm. in text.||||||
37212|Khasta Formation|24617|5|Briefly described|p114, p115 Fig. 3, p115, p125 Fig. 10|Eocene|Eocene|Conformably overlies Pidinga Formation. Geological Province: Eucla Basin. Well sorted fine-medium sandstone and siltstone, locally with carbonaceous mudstone, and/or sponge spicules facies.||||||
37212|Khasta Formation|61234|4|Described|p6, p7 Fig 4.|Late Eocene|Late Eocene|Overlain by Garford Formation; underlain by Pidinga Formation? Geological Province: Eucla Basin. Estuarine clastics.||||||14-MAY-07
37212|Khasta Formation|61814|5|Briefly described|p26|Eocene|Eocene|Estuarine sands. Geological Province: Gawler Craton.||||||08-FEB-10
37212|Khasta Formation|61839|5|Briefly described|p227|Eocene|Eocene|Estuarine sands. Geological Province: Gawler Craton.||||||14-MAY-07
37212|Khasta Formation|61856|5|Briefly described|p300 Fig.2, p304, p312-313, p315, p317|Late Eocene|Late Eocene|Consists of the former Bring Member of the Pidinga Formation, and Khasta Member of the Hampton Sandstone.|||||Very fine- to medium-grained sandstone and siltstone, with parallel and ripple lamination, lenticular and crossbedding, and marine trace fossils; local fine-grained spicule-rich sand.|
37212|Khasta Formation|64646|6|Mentioned|p23 Fig. 3|Oligocene|Late Eocene|Geological Province: Gawler Craton.||||||08-FEB-10
37212|Khasta Formation|65194|6|Mentioned|p170|Late Eocene|Late Eocene|Shows evidence of a tidal setting; sponge-spicule bearing, very fine- to medium-grained sands. Gradationally overlies Pidinga Formation. Silicified and ferruginised in Oligocene.||||||
37212|Khasta Formation|67462|5|Briefly described|Map legend.|Eocene|Eocene|Eucla Basin.||||||
37212|Khasta Formation|68715|6|Mentioned|p30 Fig.5|Priabonian|Priabonian|SW and NW Gawler Craton, Eucla Basin.||||||
37212|Khasta Formation|69004|6|Mentioned|p34|||Kingoonya Palaeovalley.||||Overlies the Pidinga Formation.||
37212|Khasta Formation|69598|6|Mentioned|p9|Early Oligocene|Late Eocene|||||Overlies the Pidinga Formation.||
37212|Khasta Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone|
23697|Kiana Granite|22629|5|Briefly described|p148|||||||||
23697|Kiana Granite|23491|6|Mentioned|p20 Fig. 4||Archean|Age: 2540 Ma. Intrudes Hall Bay Volcanics. See also p18. Of Dutton Suite.||||||07-NOV-08
23697|Kiana Granite|37620|6|Mentioned|p8|||||||||
23697|Kiana Granite|37811|6|Mentioned|Fig.3|||||||||
23697|Kiana Granite|39352|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
23697|Kiana Granite|39802|6|Mentioned|Map legend|Archean|Archean|||||||07-NOV-08
23697|Kiana Granite|40448|5|Briefly described|Table 2|||||||||
23697|Kiana Granite|40644|5|Briefly described|p120 Fig. 2, p123, p124|Paleoproterozoic|Paleoproterozoic|Of Webb and Thomson (1977). Part of the Sleaford Complex; included in the Dutton Suite as presented in this paper. Intrudes the Wangary Gneisses and Coulta Granodiorite. Geological province: Gawler Craton.||||||29-APR-09
23697|Kiana Granite|41327|6|Mentioned|p6|||||||||
23697|Kiana Granite|41667|5|Briefly described|p2|||||||||
23697|Kiana Granite|43052|5|Briefly described|p38,Table 3.1|||Of Dutton Suite.||||||21-OCT-08
23697|Kiana Granite|50605|5|Briefly described|p4.2, 8.7|||Geological Province: Gawler Craton and Curnamona Province. Of the Dutton Suite (Sleaford Complex).||||||04-OCT-06
23697|Kiana Granite|61070|5|Briefly described|Map Legend|Proterozoic|Archean|Coarse-grained tabluar K-feldspar granite, with minor biotite and muscovite. Overlain by Warrow Quartzite. Emplacement age: 2459 +/- 15Ma (U-Pb Zircon). Geological Province: Gawler Craton.||||||12-JAN-10
23697|Kiana Granite|64313|5|Briefly described|p450 Fig. 1|Paleoproterozoic|Paleoproterozoic|Age: 2462+/-15Ma (U-Pb zircon). Geological province: Gawler Craton.||||||09-FEB-10
23697|Kiana Granite|64828|5|Briefly described|p1065 Fig. 2|||Of the Dutton Suite. Included in the Sleaford Complex also. Age: 2466+/-11Ma and 2462+/-15Ma (Fanning et al 2007).||||||04-MAR-09
23697|Kiana Granite|65376|4|Described|p15, pp19-22. |||K-feldspar phenocrysts up to 50mm in length and flow-aligned.|2466 +/- 11 Ma to 2462 +/- 15 Ma.|Unit in Dutton Suite.||Intrudes Coulta Granodiorite and Hall Bay Volcanics. Is unconformably overlain locally by Warrow Quartzite.|Coarse-grained, porphyritic, tabular K-feldspar granite.|
23697|Kiana Granite|66302|6|Mentioned|p14|Siderian|Siderian|Ages are SHRIMP U-Pb from Fanning et al. (2007).|2466 +/- 11 Ma to 2462 +/- 15 Ma |Dutton Suite||||
23697|Kiana Granite|68128|6|Mentioned|p5, p7|||Gawler Craton.||Sleaford Complex||||
23697|Kiana Granite|68131|5|Briefly described|p65||||c.2460 Ma.|||Equivalent to Sir Isaac Granite.||
23697|Kiana Granite|69048|5|Briefly described|p1, p4, p6-12, p74|Paleoproterozoic|Paleoproterozoic|Southern Eyre Peninsula. Crops out at Mount Dutton and Kellidie Bay. Associated with the c.2240 Ma Sleafordian Orogeny. SHRIMP U-Pb zircon magmatic age. A previous age determination of 2462 +/- 15 Ma is discussed and rejected.|2480 +/- 4 Ma.|Dutton Suite.|||Dominantly a K-feldspar megacrystic granite. Shows moderately pervasive foliation, locally overprinted by narrow shear bands.|
23697|Kiana Granite|71859|5|Briefly described|p8-p10|Neoarchean|Neoarchean|Southern Eyre Peninsula.|c. 2480 Ma (Jagodzinski et al., 2012)|Dutton Suite||Intrudes Wangary Gneiss, Hall Bay Volcanics|Grey, K-feldspar-plagioclase-quartz-muscovite-biotite granite.|06-APR-23
23697|Kiana Granite|73026|6|Mentioned|p7|Paleoproterozoic|Paleoproterozoic|Southern Eyre Peninsula.|c. 2440 Ma|||Unconformably underlies the Warrow Quartzite.||
23697|Kiana Granite|73027|6|Mentioned|p7|Siderian|Siderian||c. 2440 Ma|||||
23697|Kiana Granite|73104|6|Mentioned|p1-2, p52, p76|Siderian|Siderian|Exposed on southern Eyre Peninsula.|c. 2480-2460 Ma|Dutton Suite, Sleaford Complex.||Equivalent to Sleaford Complex.||
23697|Kiana Granite|73230|6|Mentioned|p15|||Likely temporal correlative of Aurora Tank Suite.||Dutton Suite, Sleaford Complex||||
24335|Kilburn Sand|22888|6|Mentioned|P36|||||||||
24335|Kilburn Sand|41506|2|Defined|p9|Pleistocene||||||||
24335|Kilburn Sand|44133|6|Mentioned|p230|||||||||
83689|Kinchina adakite|73430|5|Briefly described|p508, p517-518|||Adelaide Hills. Interleaved with mafic tholeiite sills in outcrop. Strongly fractionated and HREE-depleted with Eu-anomaly-free REE patterns. High eNd values indicate a mafic source. See also name variations Kinchina/Monarto adakite p490, p516 Fig.19, p519, Kinchina Quarry Adakite p497 Fig.5, Kinchina Adakite p513 Fig.15. U-Pb monazite age of 495.0 +/-1.6 Ma of an adakite granite from Monarto Kinchina Quarry given in Table 3, p496. Generated from the delamination of a mafic, crustal underplate that was re-melted. [Also shown as Kinchina-Monarto adakitic granite p497 Fig.5, Kinchina/Monarto adakites p511 Fig.12]|495+/-1.2 Ma||||Adakitic granite with a tectonic fabric.|
23700|King Gunnia Calc-Silicate Member|22500|5|Briefly described|p 1, 4, 10|||Of the Paragon Group.||||||11-SEP-07
23700|King Gunnia Calc-Silicate Member|22553|5|Briefly described|fig2p77|Proterozoic|Proterozoic|Part of Willyama Supergroup.||||||11-SEP-07
23700|King Gunnia Calc-Silicate Member|22771|6|Mentioned|Table12.2p45|||||||||
23700|King Gunnia Calc-Silicate Member|22884|5|Briefly described|p43 Fig. 3, p47|||Within a unit of the Paragon Group. Geological province: Broken Hill Domain. May correlate to the Telechie Sulphide Member.||||||26-MAR-09
23700|King Gunnia Calc-Silicate Member|22965|6|Mentioned|Fig 1||Statherian|Within the Cartwrights Creek Metasediments.||||||
23700|King Gunnia Calc-Silicate Member|22967|6|Mentioned|p39||Statherian|||||||
23700|King Gunnia Calc-Silicate Member|38969|4|Described|p210|||||||||
23700|King Gunnia Calc-Silicate Member|39662|2|Defined|p436|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
23700|King Gunnia Calc-Silicate Member|40290|6|Mentioned|Fig.2|||||||||
23700|King Gunnia Calc-Silicate Member|40822|6|Mentioned|Fig.2|||||||||
23700|King Gunnia Calc-Silicate Member|41093|6|Mentioned|p252|||||||||
23700|King Gunnia Calc-Silicate Member|41630|6|Mentioned|Fig.1.3|||||||||
23700|King Gunnia Calc-Silicate Member|42529|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
23700|King Gunnia Calc-Silicate Member|42531|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
23700|King Gunnia Calc-Silicate Member|42537|4|Described|p15|||||||||
23700|King Gunnia Calc-Silicate Member|43086|6|Mentioned|Fig.3|||||||||
23700|King Gunnia Calc-Silicate Member|43265|5|Briefly described|Map Legend||Paleoproterozoic|Of Cartwrights Creek Metasediments||||||07-NOV-08
23700|King Gunnia Calc-Silicate Member|43266|5|Briefly described|Map Legend||Paleoproterozoic|Of Cartwrights Creek Metasediments.||||||07-NOV-08
23700|King Gunnia Calc-Silicate Member|43269|5|Briefly described|Map Legend||Paleoproterozoic|Of Cartwrights Creek Metasediments.||||||07-NOV-08
23700|King Gunnia Calc-Silicate Member|43572|6|Mentioned|Fig.3.2 p6|||||||||
23700|King Gunnia Calc-Silicate Member|50045|5|Briefly described|p116 Fig. 3|Statherian|Statherian|Geological Province: Broken Hill Block. Of Cartwrights Creek Metasediments (Paragon Group, Willyama Supergroup).||||||31-MAY-07
23700|King Gunnia Calc-Silicate Member|50619|5|Briefly described|p178 Fig. 3|Paleoproterozoic|Paleoproterozoic|Of Cartwights Creek Metasediments (Paragon Group).  Geological Province: Broken Hill Block.||||||07-NOV-08
23700|King Gunnia Calc-Silicate Member|61606|5|Briefly described|p4 Fig. 2|||Of Cartwrights Creek Metasediments.||||||
23700|King Gunnia Calc-Silicate Member|61735|5|Briefly described|p635 Fig. 1, p639 Tb. 1|Statherian||Of Cartwrights Creek Metasediments (Paragon Group). Age: 1647+/-8 Ma U/Pb SHRIMP minimum crystallisation and 1651+/-8 Ma stratigraphic age. Presented as King Gunnia CS only in Fig. 2.||||||04-JUN-15
23700|King Gunnia Calc-Silicate Member|61736|5|Briefly described|p666 Fig. 3|Paleoproterozoic|Paleoproterozoic|Of Cartwrights Creek Metasediments (Paragon Group). Geological province: Broken Hill Domain.||||||
23700|King Gunnia Calc-Silicate Member|62535|5|Briefly described|p666 Fig.3, p671-672, p674|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain. Appears as King Gunnia calc-silicate member on p671, p674.||Cartwrights Creek Metasediments.|||Metamorphosed, laminated dolomitic carbonate sediment.|
23700|King Gunnia Calc-Silicate Member|62536|5|Briefly described|p636, 639, 650-651|||Broken Hill area. Appears only as King Gunnia CS on p636. Up to 10m thick.|1647 +/- 8 Ma (min. crystall'n age).||||Laminated, sandy dolomitic (now tremolite-zoisite-rich) rocks.|
23700|King Gunnia Calc-Silicate Member|62993|6|Mentioned|p37|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain.||Cartwrights Creek Metasediments||||
23700|King Gunnia Calc-Silicate Member|63489|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Within the Paragon Group. Included in the dark, planar-layered amphibole-rich rocks of the Paragon Group.||||||07-NOV-08
23700|King Gunnia Calc-Silicate Member|63519|5|Briefly described|p6 Fig. 2, p10 Fig. 3|Paleoproterozoic|Paleoproterozoic|Of Cartwrights Creek Metasediments. Geological Province: Broken Hill Block-Euriowie Block.||||||07-NOV-08
23700|King Gunnia Calc-Silicate Member|63866|5|Briefly described|p36, p38|||Broken Hill Domain, Curnamona Province||Cartwrights Creek Metasediments||Overlain by the Bijerkerno Metasediments.||
23700|King Gunnia Calc-Silicate Member|64097|5|Briefly described|p303|Paleoproterozoic|Paleoproterozoic|Of Cartwrights Creek Metasediments (Paragon Group).||||||07-FEB-11
23700|King Gunnia Calc-Silicate Member|64741|5|Briefly described|p301 Fig. 4, p311|Paleoproterozoic|Paleoproterozoic|Of Cartwrights Creek Metasediments (Paragon Group). Geological province: Broken Hill Domain. Has stratiform-stratabound Zn-dominated mineralisation||||||07-FEB-11
23700|King Gunnia Calc-Silicate Member|64742|6|Mentioned|p321 Fig.3.|||||Unit in Paragon Group.||||
23700|King Gunnia Calc-Silicate Member|64944|5|Briefly described|p28 Fig. 1|Paleoproterozoic|Paleoproterozoic|Of Paragon Group. Geological province: Broken Hill Domain.||||||07-FEB-11
23700|King Gunnia Calc-Silicate Member|66302|5|Briefly described|p36 Fig.9, p40|Statherian|Statherian|Broken Hill Domain, Curnamona Province. ||Cartwrights Creek Metasediments||||
23700|King Gunnia Calc-Silicate Member|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Broken Hill Domain. The rank [Member] is omitted.||Cartwright Creek Metasediments.||||
23700|King Gunnia Calc-Silicate Member|70000|5|Briefly described|p37|Statherian|Statherian|Mis-spelt as King-Gunnia Calc-silicate Member.||Unit in Cartwrights Creek Metasediments.|||Thinly-bedded unit.|
23700|King Gunnia Calc-Silicate Member|70014|5|Briefly described|Map legend|||||Unit in Cartwrights Creek Metasediments.|||Layered, dark, graphitic, amphibole-rich rock. Layering thin (2-100mm), planar, continuous. Minor quartz and plagioclase-rich layers. Interpreted as a metamorphosed carbonaceous limestone.|
23700|King Gunnia Calc-Silicate Member|70657|5|Briefly described|p13 Fig.6, p15, p42, p65|Statherian|Statherian|Curnamona Province; Broken Hill Domain. Appears as King Gunnia Calc-silicate Member in Fig.6, and as King-gunnia Calc-Silicate Member [!] on p42.||Cartwrights Creek Metasediments.||||
23700|King Gunnia Calc-Silicate Member|70658|6|Mentioned|p15|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain, Curnamona Province.||Cartwrights Creek Metasediments.||||
23700|King Gunnia Calc-Silicate Member|71968|5|Briefly described|p5,18,28|Paleoproterozoic|Paleoproterozoic|Geological province: Curnamona province. ||Unit of Cartwrights Creek Metasediments.||||
23700|King Gunnia Calc-Silicate Member|72461|6|Mentioned|p16 fig 9|||||Cartwrights Creek Metasediments||||
23700|King Gunnia Calc-Silicate Member|73482|5|Briefly described|p422 Fig.3|||Shown as King Gunnia CS Member.||Cartwrights Creek Metasediments||||
23700|King Gunnia Calc-Silicate Member|73575|6|Mentioned|p828 Fig.2, p829 Fig.3|||||Cartwrights Creek Metasediments||||
37493|Kingoonya Member|24396|4|Described|p218 Fig.3, p223|Early Pliocene|Middle Miocene|Of Garford Formation.  See also p222 Fig.5. Geological Province: Gawler Craton.||||||
37493|Kingoonya Member|24606|5|Briefly described|p958 Fig. 3, p959|Middle Miocene|Middle Miocene|Of the Garford Formation. Geological Province: Eucla Basin.||||||
37493|Kingoonya Member|60497|5|Briefly described|p42|Early Pliocene|Middle Miocene|Of the Garford Formation. Geological Province: Eucla Basin.||||||
37493|Kingoonya Member|61234|4|Described|p6, p7 Fig 4.|Early Pliocene|Middle Miocene|Of the Garford Formation. Geological Province: Eucla Basin. Marginal marine-estuarine carbonaceous clastics.||||||14-MAY-07
37493|Kingoonya Member|64646|6|Mentioned|p23 Fig. 3|Pliocene|Late Miocene|Of Garford Formation. Geological Province: Gawler Craton.||||||08-FEB-10
37493|Kingoonya Member|65194|6|Mentioned|p171|Early Pliocene|Middle Miocene|Of Garford Formation; characterised by marine and estuarine influences.||||||
37493|Kingoonya Member|67462|5|Briefly described|Map legend.|Early Pliocene|Late Miocene|Eucla Basin.||Unit in Garford Formation.||||05-DEC-13
37493|Kingoonya Member|68715|6|Mentioned|p30 Fig.5|Pliocene|Pliocene|SW and NW Gawler Craton, Eucla Basin. Early Pliocene age.||||||
37493|Kingoonya Member|69004|6|Mentioned|p32|Micoene|Miocene|Kingoonya Palaeovalley.||Garford Formation||Overlies the Pidinga Formation.||
37493|Kingoonya Member|69598|6|Mentioned|p9|Late Miocene|Late Miocene|||||||
24336|Kingscote Limestone|38699|3|Fully described|p10|||||||||
24336|Kingscote Limestone|38702|5|Briefly described|p127|||||||||
24336|Kingscote Limestone|41076|6|Mentioned|Fig.11|||||||||
24336|Kingscote Limestone|41513|6|Mentioned|p43|||||||||
24336|Kingscote Limestone|41626|6|Mentioned|p50|||||||||
24336|Kingscote Limestone|44133|5|Briefly described|p165|Early Miocene|Middle Eocene|Geological Province: Saint Vincent Basin.||||||
24336|Kingscote Limestone|61155|5|Briefly described|p3, p17|Late Oligocene|Late Eocene|Widespread fossiliferous bioclastic carbonates. Age: 40-26.5Ma. Max. thickness: 40m. Geological Province: St Vincent Basin.||||||
24336|Kingscote Limestone|64282|5|Briefly described|Map legend|Oligocene|Eocene|Geolocial Province: St Vincent Basin. Comprises an upper cross-bedded calcarenite (Oligocene) and lower echinoid, bryozoan and molluscan limestone (Eocene).||||||24-JUL-08
24336|Kingscote Limestone|65891|6|Mentioned|p221 Fig.5. |Paleogene|Paleogene|Southern St Vincent Basin.||||||
24336|Kingscote Limestone|69372|6|Mentioned|p26, p28 fig. 6, p29 fig. 7, p34 Fig.12|Oligocene|Eocene|||||Overlies Cape Jervis Formation|Limestone.|
24336|Kingscote Limestone|70722|5|Briefly described|p216-217,221-230|Oligocene|Eocene|Kangaroo Island. Thickness: ~41m. Can be subdivided into 4 subunits: K1-K4 (this study). Alternatively can also be divided into lower, middle and upper sections (Lindsay and Allen 1995). Depositional environment: Quiet water, warm-temperate to subtropical marine sediments. Thin biofragmental carbonates variably altered by diagenesis, as evidenced by well cemented Oligocene limestones. Overlain by Miocene and Pliocene limestones. Subsequently uplifted in early Pleistocene and subject to meteoric alteration since.||||||
24336|Kingscote Limestone|73107|5|Briefly described|Map legend.|Oligocene|Eocene||||||Lower part: echinoid, bryozoan and molluscan limestone. Upper part: cross-bedded calcarenite.|
27065|Kirwan Siltstone|37854|6|Mentioned|Table 1|||||||||
27065|Kirwan Siltstone|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Willouran||||||
27065|Kirwan Siltstone|39348|6|Mentioned|Map legend|Adelaidean|Adelaidean|Willouran||||||
27065|Kirwan Siltstone|40225|4|Described|Map sheet|||||||||
27065|Kirwan Siltstone|40294|3|Fully described|p21|||||||||
27065|Kirwan Siltstone|41403|5|Briefly described|p67|||||||||
27065|Kirwan Siltstone|42222|6|Mentioned|Table 1 P5|||||||||
27065|Kirwan Siltstone|42882|5|Briefly described|Fig.2, P4|||of Callanna Group||||||
27065|Kirwan Siltstone|43052|5|Briefly described|p175,Table 6.1|||of Curdimurka Subgroup.||||||
27065|Kirwan Siltstone|60959|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Of the Curdimurka Subgroup. Dark grey to black, finely laminated carbonaceous siltstone; locally silicified.||||||
27065|Kirwan Siltstone|72492|5|Briefly described|p2 Fig.1, p3,  p4 Fig.3b, p6-8,|Neoproterozoic|Neoproterozoic|Possibly comparable to the Boorloo Siltstone in the Willouran Ranges. See also p7 Tb.1, p9, p10 Tb.2, p11, p12 Tb.4, p14 Tb.4, p15 Fig.9a, p16 Fig.10a, p16-17. Misspelt Kirwan Silstone p2. Coordinates are provided.||Curdimurka Subgroup||Overlies Arkaba Hill Beds and underlies Waraco Limestone.|Includes black shale and consist of plane-laminated silty shales, often with alternating silt and shale laminae.|16-SEP-20
27065|Kirwan Siltstone|73222|6|Mentioned|p7|Tonian|Tonian|Flinders Ranges. Torrensian.||Curdimurka Subgroup, Callanna Group, Warrina Supergroup||Underlain by Arkaba Hill Beds. Overlain by Waraco Limestone. Possibly equivalent to Boorloo Siltstone.||
26668|Konkaby Basalt|24472|5|Briefly described|p5 Tb.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Harris Greenstone Domain, Gawler Craton.||||||
26668|Konkaby Basalt|42469|4|Described|p16|||Variation of Konkoby Basalt, on Tarcoola map 85/24803.||||||
26668|Konkaby Basalt|42546|5|Briefly described|Map legend|Mesoproterozoic||||||||
26668|Konkaby Basalt|42736|5|Briefly described|map legend|Mesoproterozoic||||||||
26668|Konkaby Basalt|43052|5|Briefly described|p113|||||||||
26668|Konkaby Basalt|44935|5|Briefly described|Map Legend||Proterozoic|||||||
26668|Konkaby Basalt|63398|5|Briefly described|p670 Fig. 6d|Mesoproterozoic|Mesoproterozoic|Age: ca 1595Ma. Geological Province: Gawler Craton. ||||||
26668|Konkaby Basalt|64137|6|Mentioned|p1553 Fig.8 |||Neodymium isotope data.||||||
26668|Konkaby Basalt|67058|5|Briefly described|p479 Fig. 3|Mesoproterozoic|Mesoproterozoic|Gawler Craton|||||Andesite-basalt; dacite, vesicular, agglomeratic, tuffaceous.|19-APR-12
26668|Konkaby Basalt|70659|4|Described|p5-6, p8|Mesoproterozoic|Mesoproterozoic|500m thick with total area of 225 km2.||Lower Gawler Range Volcanics.||Locally intercalated with Ealbara Rhyolite.|Porphyritic to amygdaloidal basalt.|
26668|Konkaby Basalt|70738|6|Mentioned|p186-187|||Gawler Craton. Crops out in the Tarcoola-Kingoonya area.||||||
26668|Konkaby Basalt|70816|6|Mentioned|p4-5|||Tarcoola-Kingoonya area, Gawler Ranges.||Unit of lower Gawler Range Volcanics.||||
26668|Konkaby Basalt|72090|6|Mentioned|p12|||Gawler Craton.||Gawler Range Volcanics, Lower||||
26668|Konkaby Basalt|73110|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|||Lower Gawler Range Volcanics.||||
79312|Koolka Ironstone Member|70339|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|||Of Peryhumuck Formation.|||Ironstone, magnetite-rich.|
79312|Koolka Ironstone Member|70405|6|Mentioned|p23|Paleoproterozoic|Paleoproterozoic|Has not been mapped in detail.||Peryhumuck Formation|||Ironstone.|
80749|Koomalboogurra Suite|72242|5|Briefly described|p27,29-31|Statherian|Statherian|Geological province: Coompana Province. Oldest rocks dated in the Coompana Supersuite (c. 1618 Ma; Dutch 2018; Jagodzinski and Bodorkos 2018; Wingate et al. 2015a). Interpreted as subduction-related granites developed on the edge, or outboard of Gawler Craton (Dutch 2018; Swain et al. 2008). Age and geochemistry are comparable to Saint Peter Suite.|c. 1618 Ma|Unit of Toolgana Supersuite.|||Granodioritic-monzogranitic gneiss, migmatitic orthogneiss.|
80749|Koomalboogurra Suite|72344|5|Briefly described|p3, p7, p9, p17, p98|Statherian|Statherian|Coompana Province. Intersected in CDP001 and CDP006. Metamorphosed at 1163 +/- 8 Ma (SHRIMP; this volume). 3 samples dated. Petrography, SHRIMP analyses and geochemistry are discussed for a sample.|1618 +/- 6 Ma; 1618 +/- 9 Ma SHRIMP U-Pb magmatic|Of Toolgana Supersuite.|||Granodioritic-monzogranitic gneiss-migmatitic orthogneiss.|04-SEP-19
80749|Koomalboogurra Suite|72947|2|Defined|p7-11, p14, p18, p21|Statherian|Statherian|Coompana Province, eastern. Named after Koomalboogurra Cave. No known surface exposures. Type locality: CDP001 (drillhole number 299055, interval 488.53-555.5 m). Age listed is of the igneous protolith. Age of high-grade metamorphism [and partial melting]: 1163 +/- 8 Ma (SHRIMP U-Pb [?]). Interpreted to represent subduction-related granites that developed on the edge, or outboard of the Gawler Craton (Dutch et al., 2016; Swain et al., 2008). The unit can be confidently traced as an eastward-thickening wedge between the Palinar Shear Zone and the coast, to east of Albala-Karoo Bore, where it is covered by basaltic lava flows. Sheared contact with the Palinar Shear Zone in the north. The heterogeneous components form a spectrum between compositional and textural end-members. Contact between uniform and less well preserved banding is transitional and difficult to precisely define. Varying degrees of selective alteration. Similar in age and composition to the St Peter Suite.|1618 +/- 6 Ma, 1618 +/- 9 Ma SHRIMP U-Pb|Toolgana Supersuite||Intruded by Giants Head Suite and Warbla Suite, appears to be intruded by Gilgerabbie Suite. Overlain by Mallabie Basalt and Madura Formation.|Granodioritic to monzogranitic migmatitic rocks. Uniformly layered orthogneisses with regular banding transitioning to more heterogeneous gneisses with less well preserved layering. Incl: quartz, feldspar, biotite, hornblende, magnetite, garnet.|29-NOV-22
80749|Koomalboogurra Suite|73084|6|Mentioned|p123|||||Toolgana Supersuite||||
80749|Koomalboogurra Suite|73091|5|Briefly described|map legend|Statherian|Statherian||c. 1618 Ma||||Granodioritic-monzogranitic gneiss-migmatitic orthogneiss.|30-NOV-21
80749|Koomalboogurra Suite|73224|5|Briefly described|p42|Statherian|Statherian|Coompana Province, southeast domain. Similar in age and composition to the St Peter Suite. Corresponds to a northeast-trending planar magnetic grain. Protoliths were generated in a proximal back-arc at c. 1618 Ma and metamorphosed between C. 1163-1140 Ma.|c. 1618 Ma||||Migmatitic orthogneisses.|
80749|Koomalboogurra Suite|73225|5|Briefly described|p10, 13|||Southern Coompana Province.|c.1618 Ma.|Toolgana Supersuite.|||Metatexites and gneisses. Leucosomes are locally (recumbent)-folded.|
80749|Koomalboogurra Suite|73641|5|Briefly described|p2|||Subduction setting.|1620 Ma|Toolgana Supersuite||Is intruded by Giants Head Suite.|Gneisses; monzogranite.|
80747|Koonalda Suite|72242|5|Briefly described|p29-31|Stenian|Stenian|Geological province: Madura and Musgrave provinces. Associated with Maralinga Event (including Musgrave Orogeny). Massive porphyritic monzo- to syenogranitic intrusions intruded in CDP003 and CDP005 drillholes. Contains relative juvenile EHF1074Ma values and suggests little to no assimilation of pre-1900 Ma crust; appears to be product of mantle input and crustal assimilation similar to Bunburra and Koomalboogurra suites (Dutch 2018).|c. 1150 Ma|Unit of Moodini Supersuite.|||Megacrystic monzogranite-syenogranite|29-NOV-22
80747|Koonalda Suite|72344|5|Briefly described|p3, p7-p9, p50|Stenian|Stenian|Coompana Province. CA-TIMS date is interpreted as the preferred magmatic age for a sample of megacrystic syenogranite of this unit intersected in CDP003.|1149.96 +/- 0.28 Ma (CA-TIMS date)|Moodini Supersuite|Includes the Alballa-Karoo Syenogranite and Merdayerrah Shoshonite.||Massive, coarsely porphyritic syenogranite composed of large, flesh-pink K-feldspar phenocrysts in a medium grained groundmass of quartz, plagioclase and ferromagnesian aggregates.|04-SEP-19
80747|Koonalda Suite|72947|2|Defined|p7-9, p11-12, p14-18, p21|Stenian|Stenian|Coompana Province, eastern. Named after Koonalda Cave. No known surface exposures. Type locality: CDP003 (drillhole 299057, interval 345.69-411.76 m). Samples dated using SHRIMP U-Pb at 1147 +/- 9 Ma and 1140 +/- 8 Ma, and CA-TIMS 1149.96+/-0.28 Ma. A sample of adamellite from Mulyawara 1 drillhole was dated at 1168 +/- 6 Ma. Represent high-grade metamorphism, anatexis, deformation and magmatism. Relatively juvenile eHf1174-1140 Ma values suggest little or no assimilation of any pre-1900 Ma crust; appear to be the product of mantle input and assimilation of crust (Dutch, 2018). Ovoidal, fine- to medium-grained mafic enclaves present. Forms a series of overlapping, elongate elliptical plutons generally aligned with and restricted to a corridor between the Palinar and Border shear zones that extends from the coastline near the SA-WA border northeast to the northern margin of the Gawler Craton. Locally, the plutons intrude across the bounding shear zones.|~1168 - 1140 Ma|Moodini Supersuite|Includes Albala-Karoo Syenogranite.|Contemporaneous with and intruded by the Albala-Karoo Syenogranite. Intruded by Giants Head Suite and Warbla Suite. Nonconformably overlain by Loongana Formation.|Pink to green, massive, very coarse- to fine-grained (locally megacrystic) and porphyritic to inequigranular syenogranite to granodiorite.|
80747|Koonalda Suite|73084|6|Mentioned|p127|Stenian|Stenian|Age from Jagodzinski and Bodorkos (2018).|1148 +/- 7 Ma|Moodini Supersuite|||Massive porphyritic monzogranitic to syenogranitic intrusions.|
80747|Koonalda Suite|73091|5|Briefly described|map legend|Stenian|Stenian||c. 1150 Ma|Moodini Supersuite|||Megacrystic monzogranite-syenogranite.|30-NOV-21
80747|Koonalda Suite|73224|5|Briefly described|p42|Stenian|Stenian|Product of mantle input and the assimilation of crust similar to the Bunburra and Koomalboogurra suites.|c. 1150-1140 Ma|Moodini Supersuite|||Felsic composition.|
80747|Koonalda Suite|73225|6|Mentioned|p4||||||Moodini Supersuite.|||
80747|Koonalda Suite|73641|6|Mentioned|p2, 4|||||Moodini Supersuite||Is intruded by Giants Head Suite.||
77228|Kooringa Member|66522|2|Defined|pp19-33.|Neoproterozoic|Neoproterozoic|Rich epigenetic copper mineralisation from felsic porphyry lenses led to develoment of Burra mines. 182 m thick in type section. Type section described. Basal boundary taken at first siltstone. Top boundary gradational, possibly interfingering with Skillogalee Dolomite.|Mid Torrensian. 788 +/- 7 Ma.(LA-ICPMS age: Reid).|Unit in lower portion of Skillogalee Dolomite.|||Pyritic and volcaniclastic siltstone; interbedded siltstone and dolomite; distinctively laminated dolomite and limestone. Intensely hydrothermally altered, with copper mineralisation.|07-JUL-20
77228|Kooringa Member|73262|6|Mentioned|p586|Tonian|Tonian|Cut by an intrusive porphyry that has been dated at 794 +/- 4 Ma (Preiss et al., 2009).||Skillogalee Dolomite||||
77228|Kooringa Member|74367|5|Briefly described|p8, p18, p20|Tonian|Tonian|Defined by Preiss et al., (2009). Volcanics are suggested to be equivalent with the Boucaut Volcanics.|ca. 790 Ma|Skillogalee Dolomite, Mundallio Subgroup|||Volcaniclastic siltstone.|
73968|Koppio Metajaspilite|61556|6|Mentioned|p8|||May be equated with Upper Middleback Quartzite. Associated with amphibolites. See also Figure on p9-10.||||||21-NOV-07
39833|Korumburra Subgroup|13323|5|Briefly described|p393 Fig. 2|Albian|Albian|Of th Strzelecki Group. Non-marine arkose and volcanoclastics. Overlies Tyers River Subgroup (Strzelecki Group). Geological Province: Gippsland Basin. See also p393 Fig. 3.||||||26-JUN-06
39833|Korumburra Subgroup|24407|5|Briefly described|p13 Fig.2|||Geological Province: Gippsland Basin||||||
39833|Korumburra Subgroup|24551|6|Mentioned|p478 Fig 15.8|||Of the Strzelecki Group.||||||
39833|Korumburra Subgroup|61552|6|Mentioned|p583 Fig.2. |Albian||||Unit in Strzelecki Group.||||
39833|Korumburra Subgroup|64876|5|Briefly described|p145 Fig.2|Albian||Gippsland Basin.||Strzelecki Group.||||
39833|Korumburra Subgroup|65717|5|Briefly described|p9 Fig.2.2|Albian|Albian|||Strzelecki Group|||Interbedded sandstone, siltstone and shale.|05-SEP-17
39833|Korumburra Subgroup|65973|6|Mentioned|p171|||Gippsland Basin.||||||
39833|Korumburra Subgroup|70076|5|Briefly described|South-Eastern: Fig.4|Albian|Barremian|||Strzelecki Group.|Wonthaggi Formation.|Is overlain by Emperor Subgroup (Latrobe Group).||
39833|Korumburra Subgroup|75065|5|Briefly described|p151, 156-159, 172|Albian|Barremian|Bernecker and Partridge (2001). Gippsland Basin. Good hydrocarbon potential reservoir.||Strzelecki Group.|San Remo Member.|Overlies Tyers River Subgroup unconformably (onshore) and conformably (offshore). Is overlain unconformably by Emperor Subgroup. Correlates with Eumeralla Subgroup. Equivalent to Wonthaggi Formation?.|Sandstone, non-marine arkose and volcaniclastics, some coal.|
39516|Kulgera Granite|60678|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Pitjantjatjara Supersuite.  Porphyritic hornblende-biotite granite and quartz monzonite.  Geological Province: Musgrave Block.||||||
39516|Kulgera Granite|60679|5|Briefly described|Map Legend|Stenian|Stenian|Of Pitjantjatjara Supersuite. Granite monzonite, quartz monzonite. Geological Province: Musgrave Block.||||||
39516|Kulgera Granite|61154|2|Defined|p43 App., p13|Mesoproterozoic|Mesoproterozoic|Formerly Kulgera adamellite. Of the Pitjantjatjara Supersuite. Characterised by distinctive reddish colour, and consists of porphyritic and equigranular quartz monzonite to monzogranite, with microgranite dykes. Intruded by Alcurra Dolerite. GeolProv: Mus||||||19-JUL-05
39516|Kulgera Granite|63866|5|Briefly described|p207|||Fregon Domain, Musgrave Province.||Pitjantjatjara Supersuite||||
39516|Kulgera Granite|69436|6|Mentioned|p21:9|||Edgoose et al. (2004). Formerly Kulgera adamellite (Edgoose et al., 1993).||||||12-JUL-16
42439|Kulpitjata Suite|60678|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Pitjantjatjara Supersuite.  Variably deformed porphyritic biotite granite, minor hornblende granite. Geological Province: Musgrave Block.||||||12-JAN-05
42439|Kulpitjata Suite|60679|5|Briefly described|Map Legend|Stenian|Stenian|Of Pitjantjatjara Supersuite. Porphyritic biotite granite. Geological Province: Musgrave Block.||||||
42439|Kulpitjata Suite|61154|4|Described|p8, p42 App., p11|Mesoproterozoic|Mesoproterozoic|Of Pitjantjatjatra Supersuite. Variably deformed porphyritic biotite granite, lesser hornblende granite; incl: coarse granite and.............with accessory zircon, opaques, apatite. Underlies Dean Quar||||||03-AUG-05
42439|Kulpitjata Suite|63866|5|Briefly described|p206|Stenian|Stenian|Musgrave Province. Ages derived from Young et al, 2002.|1197 +/- 21 Ma to 1150 +/- 19 Ma|Pitjantjatjara Supersuite||||
42439|Kulpitjata Suite|69436|4|Described|p21:4, 6, 10|Mesoproterozoic|Mesoproterozoic|Young et al. (2002). Dominated the SE end of the Olia Chain, Musgrave Province. Has close affinities with the Mantarurr Suite. SHRIMP U-Pb and Kober Pb-Pb zircon dating of seven samples.|1197-1150 Ma (Young et al., 2002).|Pitjantjatjara Supersuite.||Intrudes Opparinna Metamorphics.|Variably deformed, porphyritic biotite granite, with lesser hornblende granite; locally contains flattened, stretched and recrystallised K-feldspar, and mylonite zones.|12-JUL-16
42439|Kulpitjata Suite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||granite|
42439|Kulpitjata Suite|71592|5|Briefly described|Appendix A.|||Musgrave Province. Other ages given c.1197-1191 Ma.|1150+/-19 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granite.|
32546|Kurrajong Formation|22525|6|Mentioned|p37||Pleistocene|former usage (Ward 1966) for a Middle Pleistocene Formation||||||
32546|Kurrajong Formation|23489|5|Briefly described|p43 Table 1|Pleistocene|Pleistocene|||||||
32546|Kurrajong Formation|44198|2|Defined|p34|Late Pleistocene|Late Pleistocene|||||||
32546|Kurrajong Formation|44199|2|Defined|p594-597|Quaternary|Neogene|Late Tertiary - Quaternary.||||||27-MAR-13
32546|Kurrajong Formation|44200|6|Mentioned|p.354, 355|||||||||
32546|Kurrajong Formation|65901|5|Briefly described|p176 Tab.1, p178 Fig.2|Pleistocene|Pleistocene|Merges with the base of Ochre Cove Formation. Included in Hindmarsh Clay by Firman (1967).||||Underlies Ochre Cove Formation.|Lithified, resistant breccia.|08-MAR-12
32546|Kurrajong Formation|66194|5|Briefly described|p579, p580, 583, 592, 593||Pleistocene| Grades upwards into the sediment of the Ochre Cove Formation at Sellicks Creek, but may be coeval facies variant.|||||Colluvial deposit: coarse, siliceous, resistant breccia with iron-rich mottles.|09-MAR-12
32546|Kurrajong Formation|70660|6|Mentioned|p3, p10, p20, p29-p30, p32, p42, p46|||||||||
32546|Kurrajong Formation|72450|5|Briefly described|Brochure, Brochure map|Pleistocene|Pleistocene|Developed along the front of the Willunga Fault escarpment.|||||Boulder beds, conglomerate, alluvial gravel, sandstone and clay.|
32546|Kurrajong Formation|73188|5|Briefly described|[See comments]|Pleistocene|Pleistocene|Mount Lofty Ranges. Associated with fault scarps. Type section east of Willunga. p: 319-320, 324, 330, 338, 346, 349, 351, 358.|||||Talus deposits including pebbly sands, conglomerate and sedimentary breccia variably indurated with siliceous and ferruginous cements.|
73973|Kyancutta Metajaspilite|61556|5|Briefly described|p9-10 Figure|Paleoproterozoic|Paleoproterozoic|In central Eyre Peninsula.||||||07-NOV-08
78350|Kychering Formation|67536|6|Mentioned|Map Legend|Neoarchean|Neoarchean|Gawler Craton. Harris Greenstone Belt.|ca. 2520 Ma||||Felsic volcanics, metasediments.|09-SEP-13
78350|Kychering Formation|69004|6|Mentioned|p18|||Gawler Craton.||||||
23710|Labyrinth Formation|22629|4|Described|p153, figs1,2|Statherian|Statherian|||||||
23710|Labyrinth Formation|23481|5|Briefly described|p19 Fig 1|||Geological Province: Gawler Craton.||||||
23710|Labyrinth Formation|23805|5|Briefly described|p4 Fig. 1|Paleoproterozoic|Paleoproterozoic|Geological Province: Gawler Craton.||||||07-NOV-08
23710|Labyrinth Formation|24197|6|Mentioned|p72|||Geological Province: Gawler Craton.||||||07-FEB-11
23710|Labyrinth Formation|24422|6|Mentioned|p84 Fig. 1|||Geological Province: Gawler Craton.||||||
23710|Labyrinth Formation|24472|5|Briefly described|p5 Tb.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Harris Greenstone Domain, Gawler Craton. Age: ~1723 Ma.||||||07-NOV-08
23710|Labyrinth Formation|24505|5|Briefly described|p5 Fig. 1|||Geological Province: Gawler Craton.||||||
23710|Labyrinth Formation|24597|5|Briefly described|p526 Fig. 1|Paleoproterozoic|Paleoproterozoic|Geological Province: Gawler Craton.||||||07-NOV-08
23710|Labyrinth Formation|41995|2|Defined|p15|Paleoproterozoic||||||||07-NOV-08
23710|Labyrinth Formation|42404|6|Mentioned|p32|||||||||
23710|Labyrinth Formation|42465|6|Mentioned|Map Legend|||||||||
23710|Labyrinth Formation|42469|3|Fully described|p17|||||||||
23710|Labyrinth Formation|43052|4|Described|p126|||Age of 1640 - 1600 Ma.||||||04-MAR-09
23710|Labyrinth Formation|43053|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Lithic sandstone, conglomerate, chert.||||||26-MAY-05
23710|Labyrinth Formation|43258|5|Briefly described|Map Legend||Mesoproterozoic|||||||
23710|Labyrinth Formation|43298|5|Briefly described|Map Legend||Mesoproterozoic|||||||
23710|Labyrinth Formation|43561|6|Mentioned|p1438|||||||||
23710|Labyrinth Formation|50605|6|Mentioned|p1.1|||Geological Province: Gawler Craton & Curnamona Province.||||||
23710|Labyrinth Formation|60515|6|Mentioned|p116 Fig.1 |||||||||
23710|Labyrinth Formation|60704|5|Briefly described|p686 Fig.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Gawler Craton.||||||07-NOV-08
23710|Labyrinth Formation|60953|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Age: 1723Ma. Sandstone, conglomerate, stromatolitic chert, minor rhyolite.||||||07-NOV-08
23710|Labyrinth Formation|60954|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Geological Province: Gawler Craton.||||||31-MAY-05
23710|Labyrinth Formation|61108|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|Sandstone, conglomerate, stromatolitic chert and minor rhyolite. Age: 1723 Ma.||||||07-NOV-08
23710|Labyrinth Formation|61522|5|Briefly described|p5 Fig.1|||Geological Province: Gawler Craton.||||||
23710|Labyrinth Formation|61864|6|Mentioned|p16 Fig.3|||||||||
23710|Labyrinth Formation|63866|5|Briefly described|p6|||Wilgena Domain, Gawler Craton. Shallow water sedimentary rocks; at least 1000m thick.|||||Stromatolitic sedimentary rocks, volcaniclastics and volcanics.|
23710|Labyrinth Formation|64130|5|Briefly described|p1378 Fig.1, p1380 Fig.2, p1382  |Paleoproterozoic|Paleoproterozoic|Central Gawler Craton. Mis-spelt as Labrynth (Fig.1) and Labrinyth (also p1382). Age from intercalated rhyolite.|1715 +/- 9 Ma, SHRIMP zircon: Fanning et al, 2007||||Basal conglomerate overlain by quartzites and black shale packages with basaltic and felsic volcanic rocks.|
23710|Labyrinth Formation|64137|5|Briefly described|p1542 Fig.1  |Paleoproterozoic|Paleoproterozoic|||||||
23710|Labyrinth Formation|64722|6|Mentioned|Fig. 5 p.13|Proterozoic|Proterozoic|Of South Australian Craton.||||||
23710|Labyrinth Formation|64726|6|Mentioned|p83 Fig.2.|||||||||
23710|Labyrinth Formation|64739|6|Mentioned|p264 Fig.1.|||Gawler Craton.||||||
23710|Labyrinth Formation|64828|5|Briefly described|p1064 Fig. 1|Mesoproterozoic|Paleoproterozoic|Geological province: Gawler Craton.||||||04-MAR-09
23710|Labyrinth Formation|65376|5|Briefly described|p8 Fig.1.1, pp203-206.|||Rapid deposition from local sources. A thin rhyolite band was used for dating.|1715 +/- 9 Ma.||||Basal finely-laminated stromatolitic chert (after carbonate), overlain by cross-bedded pebbly sandstone to boulder conglomerate; clasts include jaspilite and cherty carbonate.|
23710|Labyrinth Formation|65390|5|Briefly described|Fig.1 p11, p22 Fig. 3|Statherian|Statherian|Of Wilgena Domain, Gawler Craton. Age of 1720 Ma given.||||||
23710|Labyrinth Formation|65485|6|Mentioned|Fig 1|Paleoproterozoic|Paleoproterozoic|||||||19-MAR-12
23710|Labyrinth Formation|65922|6|Mentioned|p13 Fig. 4|||Gawler Craton.||||||
23710|Labyrinth Formation|66302|5|Briefly described|p4 Fig.3, p22-23, p32, p45, p63, p66|Statherian|Statherian|Wilgena Domain, Gawler Craton. Interpreted to have been deposited at the same time with the Kimban Orogeny in a shallow marine/lacustrine to fluvial environment. See also p76 Fig.20. |1715 +/- 9 Ma (SHRIMP U-Pb, Fanning et al, 2007)|||Unconformably overlies the Eba Formation. Overlain by the Mentor Formation.|Basal finely-laminated chert with well preserved stromatolites, overlain by pebbly sandstone to boulder conglomerate. A thin layer of rhyolite also occurs.|
23710|Labyrinth Formation|67058|3|Fully described|p476, p478, p481 Fig.5, p483, pp494-495.|Paleoproterozoic|Paleoproterozoic|Central Gawler Craton. Includes a rhyolite dated at 1715 +/- 9 Ma (Fanning et al. 2007) which contains clasts of rounded quartzite derived from the associated clastic rocks. The rhyolite is syntectonic with Kimban Orogeny, which makes the underlying Eba Formation about 60 My older than its supposed correlative, the 1656 +/- 7 Ma Tarcoola Formation. Outcrops at the base, and 6 km southeast, of Mt Eba. Deposited rapidly, possibly in an alluvial fan. Its geochemistry is discussed in detail. The authors propose the Eba Formation as a likely source.|c.1715 Ma.|||Unconformably overlies Eba Formation.|Basal units of finely laminated chert-stromatolites overlain by cross-bedded, pebbly, sericitic sandstone to matrix-supported boulder conglomerate; local phyllites and siltstones with E-W cleavage. Includes a rhyolite.|
23710|Labyrinth Formation|67181|5|Briefly described|p632 Fig.14, p634, p635 Fig.17|Statherian|Statherian|Central Gawler Craton|ca 1715 Ma (Howard et al. 2011) |||||
23710|Labyrinth Formation|67323|5|Briefly described|Eastern Australia Time-Space Plot; p33|||Central Gawler Craton.|1715 +/- 9 Ma.||||Coarse clastic succession.|
23710|Labyrinth Formation|67536|5|Briefly described|Map Legend|Statherian|Statherian|Gawler Craton.|1723 +/- 10 Ma.||||Sandstone, conglomerate, chert, rhyolite.|
23710|Labyrinth Formation|69004|6|Mentioned|p18|||Gawler Craton.||||||
23710|Labyrinth Formation|69591|6|Mentioned|p107 Fig.2.102|||Appears in a diagram of the geodynamic setting of ~1725-1690 Ma eastern Australia.||||||
23710|Labyrinth Formation|69649|6|Mentioned|p6 Fig.4,|||||||||
23710|Labyrinth Formation|70659|5|Briefly described|p5|Palaeoproterozoic|Palaeoproterozoic|Tarcoola area. Previously thought to be synchronous with Gawler Range Volcanics. |||||Fluvial-lacustrine succession.|
23710|Labyrinth Formation|70858|6|Mentioned|p33|Paleoproterozoic|Paleoproterozoic|Gawler Craton.||||||
23710|Labyrinth Formation|71235|6|Mentioned|p26||||1715+/-9 Ma (Fanning et al., 2007)|||||
23710|Labyrinth Formation|71318|5|Briefly described|p3,22|Paleoproterozoic|Paleoproterozoic|Geological province: Gawler Craton. [Misspelt as Labrynth Formation on p3]. Sample GSSA 2017963 (porphyritic rhyolite) yielded an interpreted (weighted mean 207Pb/206Pb age) magmatic crystallisation age of 1722+\-11 Ma. Zircon characteristics, petrography, U-Pb isotopic results and geochronological interpretation are provided.|||||Porphyritic rhyolite with phenocrysts of quartz and altered feldspar in a devitrified, fine-grained groundmass.|10-DEC-19
23710|Labyrinth Formation|71341|6|Mentioned|p188 fig 7|||||||||
23710|Labyrinth Formation|71712|5|Briefly described|p411, 423, 424|Paleoproterozoic|Paleoproterozoic|Thickness: ~1000m.[Says 'at least 1000 km thick' p411. I don't think so!]. Age from interbedded  rhyolite 1715+/-9 Ma U=Pb zircon.||||Underlain by Tarcoola Formation?. 1715 +\- 9 Ma rhyolite interbedded within Labyrinth Formation suggests fault contact with Tarcoola Formation.|Metasedimetary basement sequence comprising quartzite, black shale, and mafic to felsic volcanic rocks.|
23710|Labyrinth Formation|71859|5|Briefly described|p5|||Central Gawler Craton.|c.1715 Ma||||Clastic sedimentary and bimodal volcanic rocks.|
23710|Labyrinth Formation|71862|6|Mentioned|p4|||Central Gawler Craton. Deposited during the Kimban Orogeny.|||||Clastic and bimodal volcanic rocks.|
23710|Labyrinth Formation|72459|6|Mentioned|p51|Palaeoproterozoic|Palaeoproterozoic|Wilgena, deposited in shallow localised basins.|ca. 1730-1700 Ma|||||
23710|Labyrinth Formation|73026|6|Mentioned|p11|Statherian|Statherian|Syn-Kimban Orogeny.|c. 1715 Ma||||Central Gawler Craton.|
23710|Labyrinth Formation|73027|6|Mentioned|p10|Statherian|Statherian|Contains clastic material derived from local sources in the Central Gawler Craton.|c. 1715 Ma|||||
23710|Labyrinth Formation|73030|6|Mentioned|p2149|Statherian|Statherian|Gawler Craton.||||||
23710|Labyrinth Formation|73104|6|Mentioned|p37|Statherian|Statherian|Kingoonya - Mount Eba area. Possible correlative of xenoliths found in the Nummee Granodiorite. Deposited within localised transtensional basins synchronous with compressional deformation during the c. 1740-1690 Ma Kimban Orogeny.|1715 Ma|||||
23710|Labyrinth Formation|73235|6|Mentioned|p53, p64|Statherian|Statherian|Gawler Craton. Wilgena and Harris Greenstone regions. Has a vague spatial relationship with mineralisation, which has yet to be clearly defined.|1720 Ma|||||
23710|Labyrinth Formation|73493|6|Mentioned|p716 Fig.3|||Gawler Craton.||||||
38179|Lady Jane Diorite|60704|2|Defined|p699 App.1|Mesoproterozoic|Mesoproterozoic|Age: 1582+/-30 Ma (Ar-Ar). Intrudes the Paxton Granite and Tarcoola Formation. Fine grained dykes comprising of pyroxene or hornblende with a groundmass of K-feldspar laths, fine pyroxene or hornblende, magnetite, apatite and quartz, minor plagioclase.||||||11-APR-05
38179|Lady Jane Diorite|63276|5|Briefly described|p3 Fig. 2, p14 Fig. 3|Mesoproterozoic|Mesoproterozoic|Diorite dykes which cut through the Paxton Granite and Tarcoola Formation. Age: 1582+/-5Ma.||||||
38179|Lady Jane Diorite|64137|5|Briefly described|p1541-1545, p1549 Fig.6    |Mesoproterozoic|Mesoproterozoic|See also p1552-1554, p1561-1562. Part of the Gawler Range -  Hiltaba volcano-plutonic event. Intrusion was accompanied by veining, alteration and (gold) mineralisation.|~1580 Ma.|||Intrudes Paxton Granite and Tarcoola Formation.|Narrow, aphanitic to fine-grained, locally hornblende- or pyroxene-phyric, microdiorite dykes cut by sulfide-gold mineralised quartz veins.|
38179|Lady Jane Diorite|66302|6|Mentioned|p46|Calymmian|Calymmian|Informal name. Wilgena Domain. |1590 to 1575 Ma (Budd, 2006)|Hiltaba Suite|||Diorite.|
38179|Lady Jane Diorite|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Southern Gawler Craton. Appears simply as Lady Jane.|1582 +/- 5 Ma.|||||
38179|Lady Jane Diorite|71862|6|Mentioned|p13|||||||Intrudes the Paxton Granite.||
35889|Lady Louise Suite|23347|2|Defined|p51 Tb. 1, p54-55|Statherian|Statherian|Of the Willyama Supergroup.  Age: 1.69 Ga. Intrudes Curnamona Gp, including Basso Suite. Widespread as sills+dykes in Olary Domain; includes amphibolites - more detail included.||||||29-AUG-13
35889|Lady Louise Suite|60485|5|Briefly described|p28 Fig. 2|Statherian|Statherian|Igneous suite. Geological Province: Olary Domain. Age: 1685 Ma.||||||28-APR-05
35889|Lady Louise Suite|61239|5|Briefly described|p54|||Includes mafic sills, orthogneiss.||||||
35889|Lady Louise Suite|61734|5|Briefly described|p52 Fig.2|Statherian|Statherian||1.69 Ga|||Intrudes the Curnamona Group, Saltbush Subgroup and Basso Suite.|Amphibolite and mesocratic hornblende granite.|
35889|Lady Louise Suite|62373|5|Briefly described|p502, p503 Fig.2|Paleoproterozoic|Paleoproterozoic|Suite of magmatic rocks. Age: ca. 1685 Ma. Geological Province: Curnamona Province/Olary Domain.||||||07-NOV-08
35889|Lady Louise Suite|62514|5|Briefly described|p748 Fig. 3|Mesoproterozoic|Mesoproterozoic|Intrudes the Ethiudna Subgroup (Curnamona Group). Geological Province: Olary Domain/Curnamona Province.||||||16-SEP-09
35889|Lady Louise Suite|62535|5|Briefly described|p671||||c.1685 Ma.|||Intrudes Wiperaminga Subgroup.|Mafic intrusions.|
35889|Lady Louise Suite|62592|5|Briefly described|p15, p16 Fig.2.2.|Statherian|Statherian|Olary Domain. Mafic-dominated fractionated set of intrusives.|c.1685 Ma.|||||
35889|Lady Louise Suite|62993|5|Briefly described|p4, 7,8,14,23,26,37 39,40,42|Paleoproterozoic|Paleoproterozoic|Olary Domain. At the Radium Hill tailings dam borrow pit, green amphibolitic bodies considered to be part of  the 'sedimentary amphibolites' of Sprigg (1954) are now considered to be sills of Lady Louise Suite.|~1685 Ma||Includes Woman-in-White Amphibolite|Intrudes Basso Suite|Mafic dykes.|19-DEC-21
35889|Lady Louise Suite|63102|4|Described|p13,31,35,38,40,43-44,50,53|Statherian|Statherian|Geological province: Olary Domain, Curnamona Province. Mafic magmatic suite, locally differentiated into hornblende or biotite granite. Underwent extensional deformation during Willyama Supergroup deposition. Chronostratigraphic equivalent of Hores Gneiss and Parnell Formation (Broken Hill Group).|~1685 Ma||Includes Woman-in-White Amphibolite.|Intrudes Curnamona Group.|Partly differentiated amphibolite-granite sills.|
35889|Lady Louise Suite|63186|5|Briefly described|p67 Fig. 3|Paleoproterozoic|Paleoproterozoic|Geological Province: Olary Domain, Curnamona Province. Mafic rocks.||||||07-NOV-08
35889|Lady Louise Suite|63224|6|Mentioned|p12|||Geological Province: Curnamona Province.||||||07-FEB-08
35889|Lady Louise Suite|63866|5|Briefly described|p37, p41, p49||||1685 +/- 4 Ma (Page et al., 2005b)||Includes the Woman-in-White Amphibolite.|||
35889|Lady Louise Suite|64316|5|Briefly described|p534|Paleoproterozoic|Paleoproterozoic|Term used for rocks in the Olary Domain equivalent to the ca 1685Ma mafic magmatism of the Broken Hill Block.  Age: 1685+/-6Ma (SHRIMP U-Pb, Connor and Fanning 2001).||||||07-FEB-11
35889|Lady Louise Suite|64741|5|Briefly described|p301 Fig. 4, p310|Paleoproterozoic|Paleoproterozoic|Intrudes the lower section of Saltbush Group, up as far as Raven Hill Subgroup. Age: 1685Ma. Geological province: Olary Domain.||||||07-FEB-11
35889|Lady Louise Suite|64944|5|Briefly described|p28 Fig. 1|Paleoproterozoic|Paleoproterozoic|Intrudes the Saltbush Group. Age: 1685Ma. Geological province: Olary Domain.||||||07-FEB-11
35889|Lady Louise Suite|66302|5|Briefly described|p36 Fig.9, p38|Statherian|Statherian|Olary Domain, Curnamona Province. |ca. 1685 Ma||Includes the Woman-in-White Amphibolite|Intrudes the Saltbush Group.||
35889|Lady Louise Suite|67323|5|Briefly described|Eastern Australia Time-Space Plot; p33|||Olary Domain, Curnamona Province.|1687 +/- 4 Ma.|Saltbush Group.|||Amphibolite and mafic gneiss.|
35889|Lady Louise Suite|67536|5|Briefly described|Map Legend|Statherian|Statherian|Curnamona Province.|1685 +/- 4 Ma||||Amphibolite.|
35889|Lady Louise Suite|67581|6|Mentioned|p45|||||Willyama Supergroup.||||
35889|Lady Louise Suite|67653|6|Mentioned|p4|||Geological province: Curnamona Province. ||||||
35889|Lady Louise Suite|68067|6|Mentioned|Map legend.|||Areas with higher magnetic response are mapped separately.||||||27-AUG-13
35889|Lady Louise Suite|68126|5|Briefly described|p6, p29-31|Paleoproterozoic|Paleoproterozoic|Olary Domain, Curnamona Province.|1685 +/- 4 Ma (Page et al. in prep).||||Medium-grained, black, weakly layered, hornblende-plagioclase +/- garnet amphibolite with oxidised magnetite. Local metamorphic layering. Sometimes contains coarse epidotised hornblende.|
35889|Lady Louise Suite|69654|6|Mentioned|p3|||Curnamona Province.||||||
35889|Lady Louise Suite|70339|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic||U-Pb age 1685+/-4 Ma.||||Amphibolite, quartz-bearing, locally differentiated to hornblende granite, intrusive sills and dykes, metamorphosed and deformed. Granodiorite to monzogranite, A-type affinity.|
35889|Lady Louise Suite|70340|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic||U-Pb age 1685+/-4 Ma||||Amphibolite, quartz-bearing, locally differentiated to hornblende granite, intrusive sills and dykes, metamorphosed and deformed. Granodiorite to monzogranite, A-type affinity.|
35889|Lady Louise Suite|70405|4|Described|p36, p37|Paleoproterozoic|Paleoproterozoic|The intrusion of this unit into broken hill sediments may have provided the heat source to mobilise fluids for ore formation.|1685 Ma|Kalabity Supersuite||Intrudes Broken Hill Group, Raven Hill Subgroup, Wiperaminga Subgroup, Basso Suite, Ethiunda Subgroup, Oonartra Creek Formation|Mafic dykes and lenticular sills. Mafic iron rich tholeiites, fine-medium grained amphibolites and two-pyroxene mafic granulites. Commonly massive with little to no foliation present. Some are altered into chloritic schists.|
35889|Lady Louise Suite|70657|4|Described|p12, p13 Fig.6, p15-16, p21, p30-31, p45|Statherian|Statherian|See also p47, p50-51, p58, p62-63. Conor and Fanning (2001). Olary Domain, Curnamona Province. Age-equivalent to Hores Gneiss and Parnell Formation.|1685 Ma|In Willyama Supergroup.|Woman-in-White Amphibolite.|In Willyama Supergroup. Intrudes Basso Suite, Curnamona Group (Wiperaminga and Ethiudna Subgroups). Equivalent to Parnell Formation.|Mafic (amphibolite) intrusives, locally differentiated into hornblende or biotite granite.|
35889|Lady Louise Suite|70658|5|Briefly described|p1-2, 5, 8, 11, 15, 20, 29, 32, 39, 42|Paleoproterozoic|Paleoproterozoic|Olary and Broken Hill Domains, Curnamona Province. Geochemistry briefly described.|~1685 Ma.||Woman-in-White Amphibolite.|Intrudes Peryhumuck Formation. Associated with Saltbush Group.|Mafic metagranites. Includes a thick, differentiated amphibolite-granite composite sill.|
35889|Lady Louise Suite|72454|6|Mentioned|p2 Fig.2|Mesoproterozoic|Mesoproterozoic|Part of the Olary Domain. Shown only on p2 Fig.2.||||||
35889|Lady Louise Suite|72461|6|Mentioned|p6||||1685 +/- 4 Ma|||||
35889|Lady Louise Suite|73030|6|Mentioned|p2150|Statherian|Statherian||ca. 1700-1680|||||
35889|Lady Louise Suite|73482|6|Mentioned|p422 Fig.3||||||Parnell metadolerite, Silver King metadolerites|||
35889|Lady Louise Suite|73512|5|Briefly described|p2-4, p7|Statherian|Statherian|Curnamona Province, Broken Hill Block. Emplaced at ca 1685 Ma.|ca 1685 Ma||||Mafic igneous rocks including metabasite.|
81271|Lagoon Hill Granite|71348|6|Mentioned|p200|Calymmian|Calymmian|Felsic magmatism c. 1555-1530 Ma of Fanning et al. (2007).|1555-1530 Ma|||||09-AUG-19
75890|Lake Charles Diorite|67540|3|Fully described|p25-28 Fig.1, Tbs.1,2; p36 Tb.3, p37|Calymmian|Calymmian|New name. Type locality: Drillhole LD95002, between 155.70-229.20 m. Curnamona Province: Mulyungarie Domain. Definition reference: this article and Fricke and Hore (2011). Mis-named as Lake Charles Granite in Fig.1.|1585 +/- 195 Ma (SHRIMP I, Fanning 1997)|Of the Ninnerie Supersuite.||Intrudes the Peryhumuck Formation.|Medium- to fine-grained quartz-biotite-hornblende-bearing diorites to granodiorites. I-type.|08-FEB-16
75890|Lake Charles Diorite|67900|6|Mentioned|p19, 32|||Wade (2011). Benagerie Ridge, Curnamona Province.||||||
75890|Lake Charles Diorite|69562|5|Briefly described|p671 Tb.5||||1585 +/- 195 Ma (Fanning, 1995).||||Medium- to fine-grained hornblende-bearing diorites to granodiorites.|
75890|Lake Charles Diorite|69650|2|Defined|p4 Tb.1, p6, p13, p38-45, p57|Calymmian|Calymmian|New name, after Lake Charles, 130 km NNE of Olary. Mulyungarie Domain, Curnamona Province. Type section: Drillhole LD 95 002, GDA 94, 459842 mE, 6545178 mN (Fig. 17), within the interval 155.70?229.20 m.. Subsurface: several magnetic intrusive bodies in TMI imagery and intersected in several drill holes. Appears as Lake Charles Granite in p2. Post-dates main effects of Olarian Orogeny (~1620-1580 Ma). 1585 +/- 195 Ma (SHRIMP 1, Fanning 1997). Geochemistry outlined. Disseminated and vein mineralisation (pyrite, chalcopyrite, bornite and rare molybdenite) occurs in altered diorites.|1590-1500 Ma interpreted; Fanning (1997).|Unit in Ninnerie Supersuite.||Intrudes Peryhumuck Formation.|Medium- to fine-grained, quartz-biotite-hornblende-bearing diorites to granodiorites; local carbonate, chlorite and sericite alteration. I-type.|25-NOV-22
75890|Lake Charles Diorite|70658|5|Briefly described|p33-34, 36|Mesoproterozoic|Mesoproterozoic|Curnamona Province. Subsurface Benagerie Ridge.|~1590 to 1550 Ma (Fanning, 1997).||||Medium- to fine-grained quartz-biotite-hornblende-bearing diorites to granodiorites. I-type.|
75866|Lake Elder Rhyodacite|67540|3|Fully described|p25, p27 Tb.1, p28 Tb.2, p38 Fig.2|||Type locality: Drillhole BRD003, in the interval 203.30-262.23 m. Curnamona Province: Mudguard Domain. Definition reference: Fricke and Hore (2011). |~ 1585 Ma|Of the Benagerie Volcanic Suite.|||Porphyritic, orthoclase-plagioclase-olivine (fayalite)-clinopyroxene rhyodacite with apatite, zircon and minor pyrite and chalcopyrite. A-type.|08-SEP-14
75866|Lake Elder Rhyodacite|67900|6|Mentioned|p20|||||Benagerie Volcanic Suite.||Unconformably overlies Willyama Supergroup.||
75866|Lake Elder Rhyodacite|69562|5|Briefly described|p672 Tb.5||||c.1585 Ma (Wade, 2011).|Unit in Benagerie Volcanic Suite.|||Porphyritic rhyodacitic volcanic rocks.|
75866|Lake Elder Rhyodacite|69650|3|Fully described|p4 Tb.1, p7, p13, p44, p46 Fig.2, p47-51|Calymmian|Calymmian|New name, after Lake Elder. Type section: Drillhole BRD 003, GDA 94, 445700mE, 6601900 mN (Fig. 20), in the interval 203.3?262.23 m. Geophysical imagery suggests a thick, flat-lying sheet. Geochemistry detailed. No age information.||Unit in Benagerie Volcanic Suite.||Unconformably overlies folded Willyama Supergroup. Gradationally interlayered with Finlay Dam Rhyolite.|Grey, porphyritic, orthoclase-plagioclase-olivine (fayalite)-clinopyroxene rhyodacite with apatite, zircon and minor pyrite and chalcopyrite. A-type.|25-NOV-22
75866|Lake Elder Rhyodacite|70658|5|Briefly described|p33-35|Mesoproterozoic|Mesoproterozoic|Benagerie Ridge, Curnamona Province. Geochemistry briefly described.|~1585 Ma.|Benagerie Volcanic Suite.|||Porphyritic orthoclase-plagioclase-olivine (fayalite)-clinopyroxene rhyodacite with apatite, zircon and minor pyrite and chalcopyrite. A-type.|
25145|Lake Gairdner Conglomerate|41619|6|Mentioned|Map Legend|Tertiary||||||||
25985|Lake Gairdner Rhyolite|29838|2|Defined|p11|Mesoproterozoic|Mesoproterozoic|||||||
25985|Lake Gairdner Rhyolite|35078|6|Mentioned|Fig.1|||||||||
25985|Lake Gairdner Rhyolite|42465|5|Briefly described|Map Legend|||||||||
25985|Lake Gairdner Rhyolite|42469|6|Mentioned|p16|||Gairdner, SH53-15||||||
25985|Lake Gairdner Rhyolite|42546|5|Briefly described|Map legend|Mesoproterozoic||||||||
25985|Lake Gairdner Rhyolite|42721|5|Briefly described|map legend|Carpentarian||||||||
25985|Lake Gairdner Rhyolite|42736|5|Briefly described|map legend|Mesoproterozoic||||||||
25985|Lake Gairdner Rhyolite|43052|5|Briefly described|p113|||||||||
25985|Lake Gairdner Rhyolite|43094|4|Described|p21|||see also Table 3.||||||
25985|Lake Gairdner Rhyolite|67058|5|Briefly described|p478 Fig. 2|Mesoproterozoic|Mesoproterozoic|Gawler Craton|||||Rhyolite-rhyodacite lavas, welded tuff, breccia.|19-APR-12
25985|Lake Gairdner Rhyolite|67909|5|Briefly described|p126-128, 131-132, 141|Mesoproterozoic|Mesoproterozoic|Kokatha area. Volcanic textures and emplacement mechanism tabulated.||Chitanilga Volcanic Complex.|||A multiple-flow ignimbrite unit, massive to eutaxitic texture, defined by fiamme or flattened lithics in the matrix.|
25985|Lake Gairdner Rhyolite|70659|4|Described|p6, p8|Mesoproterozoic|Mesoproterozoic|30m thick, 35 km2 total area.||Lower Gawler Range Volcanics.||Overlies Chitanilga Volcanic Complex|Rhyolitic ignimbrite.|
25985|Lake Gairdner Rhyolite|70816|5|Briefly described|p5|||Kokatha-NW Lake Gairdner area, Gawler Ranges.||Unit of lower Gawler Range Volcanics.||Underlain by Chitanilga Volcanic Complex.||
25985|Lake Gairdner Rhyolite|72090|6|Mentioned|p12|||Gawler Craton.||Gawler Range Volcanics, Lower||||
25985|Lake Gairdner Rhyolite|73110|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|||Lower Gawler Range Volcanics.||||
29820|Lake Harris Komatiite|22629|5|Briefly described|p149|Archean|Archean|2000m thick.||||||07-NOV-08
29820|Lake Harris Komatiite|24472|5|Briefly described|p5 Tb.1|Archean|Archean|Geological Province: Harris Greenstone Domain, Gawler Craton. Parent: Mulgathing Complex.||||||07-NOV-08
29820|Lake Harris Komatiite|43052|4|Described|p43, Table 3.2|||Of Mulgathing Complex||||||
29820|Lake Harris Komatiite|50605|5|Briefly described|p8.7|||Of the Mulgathing Complex. Geological Province: Gawler Craton & Curnamona Province.||||||02-APR-14
29820|Lake Harris Komatiite|63866|5|Briefly described|p4, p18|||Harris Greenstone Belt, Gawler Craton.||||Intruded by the Glenloth Granite.|Ultramafic to mafic volcanics.|
29820|Lake Harris Komatiite|64137|6|Mentioned|p1553 Fig.8 |||Neodymium isotope data.||||||
29820|Lake Harris Komatiite|65376|5|Briefly described|p190, pp194-195. |||A large (25 x 2 km), composite body, part of Harris Greenstone Belt.|c.2509 +/- 23 Ma.|Unit in Mulgathing Complex.||Discordant contact with Glenloth Granite.|Fine-grained subvertical grey to greyish black metakomatiite composed predominantly of serpentine with subordinate chlorite, tremolite, magnetite and chromite; very fine spinifex textures in upper part.|
29820|Lake Harris Komatiite|66302|6|Mentioned|p12|||||Mulgathing Complex|||Komatiite.|
29820|Lake Harris Komatiite|67536|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Gawler Craton. Harris Greenstone Belt.|ca. 2520 Ma||||Komatiite.|
29820|Lake Harris Komatiite|68128|6|Mentioned|p2-p3, p6-8|Palaeoproterozoic|Archaean|Gawler Craton. Hoatson et al (2005) suggest a depleted mantle source with little crustal contamination emplaced within an intraplate environment.|ca 2520-2510 Ma (Swain et al, 2005)|Mulgathing Complex||||
29820|Lake Harris Komatiite|69004|6|Mentioned|p18|||Gawler Craton.||||||
29820|Lake Harris Komatiite|69649|6|Mentioned|p35|Archean|Archean|Supercrustal ultramafic volcanics. Part of the basement on TARCOOLA.||||||
29820|Lake Harris Komatiite|71859|5|Briefly described|p2, p28|Neoarchean|Neoarchean|Central-western Gawler Craton.|c. 2520 Ma|Mulgathing Complex.|||Komatiitic rocks.|
29820|Lake Harris Komatiite|72459|6|Mentioned|p51||||2500 Ma|||||
29820|Lake Harris Komatiite|73230|4|Described|p6-8, p12|Neoarchean|Neoarchean|Gawler Craton. Domain: Harris Greenstone. Has locally anomalous Ni-Cu and Ni-PGE and is predominantly low in sulfer based on limited testing. Very few outcrops. Interlayered with Kenella Gneiss. Preserve characteristic extrusive textures such as ponded flows and channel facies including spinifex textures. Thought to be genetically related to Hopeful Hill Basalt via fractional crystallisation.|Older than c. 2510 Ma (magmatic)|Mulgathing Complex||Intruded [crosscut] by Glenloth Granite.|Bright green metakomatiite with illite, tremolite, chlorite and serpentine. Saprolite float.|
29820|Lake Harris Komatiite|73235|6|Mentioned|p56, p61|||Hosts gold mineralisation in the Harris Greenstone mineral field of the Sleafordian gold mineral system and in the Labyrinth mineral field of the Kararan (Gawler Range Volcanics) gold mineral system.||||||
34762|Lake Maurice Group|22922|5|Briefly described|34|||||||||
34762|Lake Maurice Group|23282|6|Mentioned|p56|||||||||
34762|Lake Maurice Group|23479|5|Briefly described|p26|||Geological Province: Gawler Craton.||||||
34762|Lake Maurice Group|24112|5|Briefly described|p254 Fig.2|Neoproterozoic|Neoproterozoic|Geological Province: Officer Basin.||||||24-SEP-08
34762|Lake Maurice Group|61732|5|Briefly described|p4 Fig. 3, p57 Fig. 21|Ediacaran|Ediacaran|Includes Tarlina Sandstone, Meramangye and Murnaroo Formations. Geological Province: southeastern Officer Basin. See also p145 Fig. 51.||||||07-FEB-11
34762|Lake Maurice Group|62453|5|Briefly described|p5 Fig. 3|Ediacaran|Cryogenian|Geological Province: Officer Basin.||||||
34762|Lake Maurice Group|63811|6|Mentioned|p501 Fig.2|||In Giles 1.||||Underlies Dey Dey Mudstone, Ungoolya Group.||28-MAR-12
34762|Lake Maurice Group|64103|6|Mentioned|p400 Fig. 3|Ediacaran|Ediacaran|Geological Province: Officer Basin.||||||07-FEB-11
34762|Lake Maurice Group|64794|5|Briefly described|p238 fig 2, p244|Ediacaran|Ediacaran|Thickens northwards across the Murnaroo Platform into the Munyarai Trough.|||Meramangye Formation, Tarlina Sandstone, Murnaroo Formation.||Coarse marine and non-marine clastics with marine mudrock wedge between halves.|
34762|Lake Maurice Group|64970|6|Mentioned|p719 Fig. 2|Neproterozoic|Neoproterozoic|Geological Province: Officer Basin.||||||27-MAY-09
34762|Lake Maurice Group|65365|5|Briefly described|p10 Fig. 4|Ediacaran|Cryogenian|Eastern Officer Basin||||||
34762|Lake Maurice Group|65366|5|Briefly described|p23 Fig. 3|Ediacaran|Cryogenian|Eastern Officer Basin||||||
34762|Lake Maurice Group|67120|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic||||||Conglomerate; siltstone, mudstone; sandstone, shale.|
34762|Lake Maurice Group|67536|6|Mentioned|Map Legend|||One of several Formations mapped collectively as N2.|||||Dominantly marine shale, siltstone, sandstone and limestone.|
34762|Lake Maurice Group|68270|5|Briefly described|p683|Ediacaran|Ediacaran|Eastern Officer Basin.||||Overlain by Ungoolya Group.||
34762|Lake Maurice Group|69003|6|Mentioned|p60|Ediacaran|Ediacaran|E Officer Basin.||||||
34762|Lake Maurice Group|69648|4|Described|p18-19, p34, map legend|Neoproterozoic|Neoproterozoic|Was Maurice Group (Zhang 1995); renamed Lake Maurice Group by Morton (1997). Age: Miranoan. Probable equivalents of this unit have been interpreted from drillhole logs. Three Formations form a complete transgressive-regressive cycle. Officer Basin was subject to relatively rapid subsidence during deposition of this Group. A major hiatus spanning ~130 million years lies between Alinya Formation and overlying Tarlina Sandstone (Lake Maurice Group).|||Basal Tarlina Sandstone, Meramangye Formation, Murnaroo Formation|Tarlina Sandstone unconformably overlies Alinya Formation (although structurally conformable).||17-FEB-15
34762|Lake Maurice Group|70336|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic||||||Conglomerate, siltstone, mudstone, sandstone, shale.|
34762|Lake Maurice Group|72476|6|Mentioned|p26, p36 Fig.9|||Officer Basin. Sediments derived from the Musgrave Block.||||||
34762|Lake Maurice Group|72478|6|Mentioned|p8|Marinoan|Marinoan|Officer Basin.|||Includes the Tarlina Sandstone, Meramangye Formation and the Murnaroo Formation.|Underlies the Ungoolya Group. Unconformably overlies the Callanna Group.||
34762|Lake Maurice Group|72601|6|Mentioned|p5|||Officer Basin.||||||
34762|Lake Maurice Group|73099|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Officer Basin.|||Tarlina Sandstone, Meramangye and Murnaroo Formations.|Overlies Alinya Formation. Is overlain by Ungoolya Group.||
25147|Lake Torrens Formation|29897|6|Mentioned|p302|||||||||
25147|Lake Torrens Formation|30056|6|Mentioned|p148|||||||||
25147|Lake Torrens Formation|31895|4|Described|Table 1|||Age||||||
25147|Lake Torrens Formation|38605|6|Mentioned|p34|||||||||
25147|Lake Torrens Formation|40439|6|Mentioned|p383|||||||||
25147|Lake Torrens Formation|41600|6|Mentioned|p828|||||||||
29675|Lamdina beds|42999|5|Briefly described|Table 2 p90|Late Triassic|Late Triassic|Paly zone T4.||||||09-APR-15
75081|Larry Macs Subgroup|62993|6|Mentioned|p14, p15, p37|Paleoproterozoic|Paleoproterozoic|Olary Domain.||Saltbush Group|Includes Bimba Formation, Plumbago Formation||Includes: Weathered pyritic calcsilicates. Fine grained, platy, graphitic psammitic schist.|17-DEC-21
75081|Larry Macs Subgroup|64741|5|Briefly described|p301 Fig. 4|Paleoproterozoic|Paleoproterozoic|Of Saltbush Group. Includes Bimba and Plumbago Formations. Geological province: Olary Domain.||||||07-FEB-11
75081|Larry Macs Subgroup|64944|4|Described|p29 Tb. 1|Paleoproterozoic|Paleoproterozoic|Of Saltbush Group. Contains Plumbago and Bimba Formations. Age: 1693+/-4Ma. Geological province: Olary Domain. Thin, regionally extensive 'couplet' of units.||||||07-FEB-11
75081|Larry Macs Subgroup|66302|5|Briefly described|p36 Fig.9, p37, p38, p39|Statherian|Statherian|Olary Domain, Curnamona Province. ||Saltbush Group|Includes the Bimba Formation and the Plumbago Formation.|||
75081|Larry Macs Subgroup|70405|4|Described|p25, p43 Table 3|Paleoproterozoic|Paleoproterozoic||1665 Ma-1700 Ma|Saltbush Group|Includes Bimba Formation and Plumbago Formation|Underlies Mount Howden Subgroup|volcaniclastic sediments and metasediments, carbonates and metacarbonates with anomalous base metal concentrations.|
75081|Larry Macs Subgroup|70657|4|Described|p13 Fig.6, p14-16, p20, p24, p33-34, p66|Statherian|Statherian|Curnamona Province, Olary Domain. Has great regional continuity. Equivalent to the interval from Clevedale Migmatite to Allendale Metasediments in the Broken Hill Group. Mineralisation described.|<1705 Ma - 1693 +/- 4 Ma|Saltbush Group|Includes Plumbago Formation, Bimba Formation.|Underlies Raven Hill Subgroup. Overlies Ethiudna Subgroup, and Portia Formation (in Mulyungarie Domain). Equivalent to Allendale Metasediments.||
75081|Larry Macs Subgroup|70658|5|Briefly described|p1-2, 7, 10, 15, 29|Paleoproterozoic|Paleoproterozoic|Olary Domain, Curnamona Province.|~1695 Ma.|Saltbush Group.|Bimba, Plumbago Formations.|Overlies Peryhumuck Formation.|Psammite, calc-silicate, marble, sulphidic rock; grey, thinly bedded fine-grained psammite.|
75081|Larry Macs Subgroup|73429|5|Briefly described|p106 Fig.2, p107|Statherian|Statherian|Curnamona Province, Olary Domain.||Saltbush Group|Bimba Formation, Plumbago Formation|Unconformably overlies Ethiudna Subgroup, underlies Raven Hill Subgroup||
34333|Laura Formation|22674|4|Described|p718, Fig.2 p719|Barremian|Barremian|||||||
34773|Lepidocyclina Limestone|22938|5|Briefly described|fig5|Miocene|Miocene|Eastern Mount Lofty Ranges.||||||
30346|Lincoln Gap Siltstone Member|70406|4|Described|p122-123, 119-121, 126|Neoproterozoic|Neoproterozoic|New name. Source given. Used to describe lower half of Corraberra Sandstone Member of Thomson (1965). ~40m thick. Deposited above storm wave base. Misspelt as Lincoln Gap Sandstone Member p121 Fig 5.||Of Tent Hill Formation||Sharply overlain by Corraberra Sandstone Member. Lateral equivalent of Moorillah Siltstone Member of Brachina Formation.|Interbedded greyish red shale and thin to medium-bedded, fine-grained greyish brown sandstone, commonly laminated.Flute casts & scratch marks common at base of sst beds, ripple marks at top.|12-MAY-16
30346|Lincoln Gap Siltstone Member|71037|5|Briefly described|p22-23 Fig.2|Neoproterozoic|Neoproterozoic|Shown only on the Six Mile Hill 1:75,000 surface geology map (p22-23 Fig.2).||Tent Hill Formation||Overlies Tregolana Shale Member and underlies Corraberra Sandstone Member.|Interbedded reddish brown laminated and ripple cross-bedded siltstone and fine-grained sandstone; flute casts.|
30346|Lincoln Gap Siltstone Member|71129|4|Described|p128-131,134,138,164,209,225|Ediacaran|Ediacaran|Of Stuart Shelf. Also referred to as Lincoln Gap Member in text. Previously known as Lincoln Gap Flagstones (Miles 1955), and interpreted to be part of Corraberra Sandstone (Thomson 1965), and seubsequently defined as a separate unit in the Tent Hill Formation by Dyson (1996). Thickness: u to 40m. Largely obscured by colluvium flanking the plateaus. Displays sedimentary structures (p129) that indicate deposition above storm wave base and below fair-weather base, and influence of unidirectional and oscillatory currents. See also app 239.||Unit of Tent Hill Formation.||Overlain disconformably by Corraberra Sandstone Member. Underlain conformably by Tregolana Shale Member. Correlable to Moorillah Siltstone Member/Brachina Fm.|Greyish brown fine-grained sandstones interbedded with greyish red shales; thin- to medium-bedded, flute casts and scratch marks at the base of beds.|13-NOV-19
30346|Lincoln Gap Siltstone Member|71131|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Age shown as Marinoan.||Tent Hill Formation.|||Interbedded reddish-brown laminated and ripple cross-bedded siltstone and fine-grained sandstone; flute casts.|
30346|Lincoln Gap Siltstone Member|73234|6|Mentioned|p6|||||Tent Hill Formation, Wilpena Group||||
24359|Linns Springs Member|40672|2|Defined|p3-p5|||See also mention P2.||||||
24359|Linns Springs Member|44133|5|Briefly described|p23|||Of the lower Mernmerna Formation. (Clarke 1986)||||||
24359|Linns Springs Member|60418|5|Briefly described|p135|Botoman-Atdabanian|Botoman-Atdabanian|Thickness: 361m. Interbedded flaggy dark grey to black limestones and shales. Of Mernmerna Formation.||||||
24359|Linns Springs Member|62784|6|Mentioned|p9|Early Cambrian|Early Cambrian|Unit in lower Mernmerna Formation of Hawker Group. Arrowie Basin.||||||20-MAR-12
24359|Linns Springs Member|63569|6|Mentioned|p119|Early Cambrian|Early Cambrian|||Unit in lower Mernmerna Formation.||||
24359|Linns Springs Member|70833|5|Briefly described|p186,198,200|Series 2|Series 2|Of Arrowie Basin.||Unit of Mernmerna Formation.||Overlain by Six Mile Bore Member. Underlain by Third Plain Creek Member.||
24359|Linns Springs Member|70835|6|Mentioned|p336|Cambrian|Cambrian|Arrowie Basin, Flinders Ranges.||Mernmerna Formation.||Overlies Six Mile Bore Member. Is overlain by Third Plain Creek Member.||
24359|Linns Springs Member|71102|5|Briefly described|p244,246,251,256|Series 2|Series 2|Of Arrowie Basin. Nomenclature of Clarke (1986b, 1990a) in the Bunkers Graben and Range; variably developed in the Arrowie Basin. Intersected sections: DBS (Donkey Bore Syncline), MMF (Bunkers Range, Central Flinders Ranges), 10MS (10 Mile South, Bunkers Graben). Variably developed within the Arrowie Basin.||Unit of Mernmerna Formation.||Overlain by Third Plain Creek Member. Undelain by Six Mile Bore Member, or disconformably by Wilkawillina Limestone.||
72904|Little Pinbong granite|63020|5|Briefly described|p987 Fig. 8|Paleoproterozoic|Paleoproterozoic|Informal name. Age: ~1670Ma. Geological Province: Gawler Craton (Coulta Domain).||||||07-NOV-08
72904|Little Pinbong granite|65390|6|Mentioned|p21, p23 Fig.3|Statherian|Statherian|Article leaves out the lithology: no explanation. Coulta Domain. Age of 1670 +/- 17 Ma (Fanning,1997) given.||||||
37190|Livingston Tillite Member|24392|2|Defined|p139, p144 Appendix 1|Valanginian|Berriasian|Of the Cadna-owie Formation. See also page 140 Fig.1  Maximum thickness: 2m.  Geological Province: Eromanga Basin.||||||
37190|Livingston Tillite Member|24510|5|Briefly described|p48|Early Cretaceous|Early Cretaceous|Of the Cadna-owie Formation. Glacial sediments. A thin tillite underlain by proglacial sediments sits near base of the Cadna-owie Formation. Type section nominated at 'Recorder Hill'.||||||04-MAY-05
37190|Livingston Tillite Member|66303|5|Briefly described|p28.|Early Cretaceous|Early Cretaceous|||Unit in Cadna-owie Formation.|||Diamictites, pebbles and coarse breccia layers.|01-MAY-15
37190|Livingston Tillite Member|67561|5|Briefly described|p52, p67|Valanginian|Berriasian|Outcrops along the southern margin of the Eromanga Basin. Constrained by the age of the Cadna-Owie Formation. Correlative of the Hooray Sandstone.||Of the lower Cadna-Owie Formation.||||01-MAY-15
37190|Livingston Tillite Member|69019|5|Briefly described|p87-88.|||Of Alley and Frakes (2003). Thickness to 2 m; laterally continuous over length of outcrop (~500 m).||Unit in Cadna-owie Formation.|||Near basal unit, massive, clasts to boulder size in a disrupted sandy-silty matrix; weakly to strongly cemented by carbonate, locally by iron oxides; rare fossil ice wedges.|
37190|Livingston Tillite Member|70383|5|Briefly described|p52|Early Cretaceous|Early Cretaceous|Crops out c.45km N of Mount Gee, at the northern margin of the Flinders Ranges.||Cadna-owie Formation.||Equivalent to Sprigg Diamictite Member.|Glacial tillites and periglacial deposits.|
37190|Livingston Tillite Member|70384|5|Briefly described|Map legend.|Early Cretaceous|Early Cretaceous|Terrigenous paludal-fluvial to transgressive marginal marine deposits. Maximum depositional age.|~120 Ma (U-Pb detrital zircons).|Of Cadna-owie Formation.|||Near-basal, thin tillite +/- rare fossil ice wedges on preglacial diamictite (silt-clay matrix, quartz grit to angular boulder framework).|23-JAN-19
37190|Livingston Tillite Member|71342|6|Mentioned|Ch6 p7|Valanginian|Valanginian|Eromanga Basin. Deposited during a short interval when glaciers formed on the margins of the basin.||Cadna-owie Formation||||
37190|Livingston Tillite Member|72456|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Marree 1:250k map sheet. |||||Tillite with disrupted, sandy, silty matrix, locally cemented by carbonate and iron oxide.|
41687|Lookout Granodiorite|24197|5|Briefly described|p75 Tb. 8.1|Mesoproterozoic|Mesoproterozoic|Age: 1560Ma.||||||07-FEB-11
41687|Lookout Granodiorite|43052|5|Briefly described|Table 4.8|||||||||
41687|Lookout Granodiorite|50605|5|Briefly described|p(iii), 1.4, 10.2, Table 1.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Gawler Craton & Curnamona Province. Of the Moolawatana Suite.||||||
41687|Lookout Granodiorite|70384|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Age uncertain.|||||Granodiorite, red-weathering, gneissic; phenocrysts of K-feldspar in a finer-grained groundmass of quartz, feldspar, plagioclase, biotite and hornblende.|
33820|Lycosa Formation|63056|5|Briefly described|p81 Fig. 2, p82|Late Cambrian|Late Cambrian|Of the Dullingari Group. Thickness: 200m. Geological Province: Warburton Basin.||||||06-FEB-07
33820|Lycosa Formation|65489|5|Briefly described|p39, p96, p120|Late Cambrian|Middle Cambrian|Eastern Warburton Basin. Gas flow from Challum 19 well.||Unit in Dullingari Group.|||Shale-dominated.|
33820|Lycosa Formation|68731|6|Mentioned|p168, p170 Fig 3.83|Late Cambrian|Middle Cambrian|~ 200 m thick.||||||
33820|Lycosa Formation|69449|6|Mentioned|p34:2 Fig.34.2|Cambrian|Cambrian|Eastern Warburton Basin.||||||12-JUL-16
33820|Lycosa Formation|69673|6|Mentioned|p149 fig 120|||||||||
33820|Lycosa Formation|69982|3|Fully described|p24, p13, p17-19, p23-27, p29, p45,|||See also p51, p54, p56-57, p142, p146, p151, p156, Appendix 1. Named after Lycosa 1 well; the type section is the interval from 2531.1 to 2724.9 m. Altered rocks of this unit were mistaken for the Merrimelia Formation during drilling of Lycosa 1 well. Contains sulfide mineralisation. Three microfacies detailed. Interpreted as a distal starved basinal turbidite deposit; a lateral facies variation of the Kalladeina Formation. Reservoir attributes described. Brief thin section descriptions. Composite logs shown.||||Is intercalated with Jena Basalt. Is overlain unconformably by Narcoonowie Formation.|Dark grey to black, horizontally laminated siltstone and shale, with abundant pyrite nodules and wavy black streaks (stylolites); deformed to produce steep dips, folds, fractures, quartz veinlets and dissolution seams.|12-NOV-15
33820|Lycosa Formation|70749|5|Briefly described|p43-45|Cambrian|Cambrian|Warburton Basin. Extends into undercover Thomson Orogen. Deep marine: starved basin sediments.|||||Finely interlaminated black pyritic shale, lime mudstone, limestone and grey to white calcareous siltstone to sandstone.|
33820|Lycosa Formation|71965|4|Described|p896,898-900,911,913|Furongian|Furongian|Geological province: Thomson Orogen. Of Warburton Basin. Widespread in the SE Warburton Basin and interpreted to be a distal turbidite deposit (Sun and Gravestock, 2001). Inferred to be of late Cambrian age (e.g. Boucher 2001; Radke 2009), but has not been biostraigraphically or geochronologically confirmed. Presence of graptolites indicate an Upper Cambrian or Lower Ordovician age. Possible minimum age provided by the intrusive Late Silurian Wolgolla Granite.|425.4 +/- 6.6 Ma (intrusive age)|Unit of Dullungari Group.||Intruded by Late Silurian Wolgalla Granite. Laterally grades into Thomson beds and Werewilka Formation.|Laminated carbonaceous mudstone.|29-OCT-19
38533|Mabel Creek Ridge paragneisses|23805|5|Briefly described|p4 Fig. 1|Paleoproterozoic|Paleoproterozoic|Geological Province: Gawler Craton.||||||07-NOV-08
38533|Mabel Creek Ridge paragneisses|24505|5|Briefly described|p5 Fig. 1|||Informal name. Geological Province: Gawler Craton.||||||
38533|Mabel Creek Ridge paragneisses|60515|6|Mentioned|p116 Fig.1 |||||||||
38533|Mabel Creek Ridge paragneisses|61522|5|Briefly described|p5 Fig.1|||Informal name. Geological Province: Gawler Craton.||||||
38533|Mabel Creek Ridge paragneisses|61659|6|Mentioned|p30 Fig.1. |Paleoproterozoic|Paleoproterozoic||||||Paragneisses.|
38533|Mabel Creek Ridge paragneisses|64739|6|Mentioned|p264 Fig.1. |Paleoproterozoic|Paleoproterozoic|Gawler Craton. Informal name.||||||
38533|Mabel Creek Ridge paragneisses|65376|6|Mentioned|p8 Fig.1.1, pp224-226.|Paleoproterozoic|Paleoproterozoic|Discordant zircon analyses do not permit accurate dating. Metamorphism occurred during the Mesoproterozoic, possibly c.1565 Ma.||||||
38533|Mabel Creek Ridge paragneisses|65390|6|Mentioned|p11 Fig.1|||||||||
38533|Mabel Creek Ridge paragneisses|65922|6|Mentioned|p13 Fig. 4|||Gawler Craton.||||||
38533|Mabel Creek Ridge paragneisses|66302|6|Mentioned|p4 Fig.3, ||||||||Paragneisses.|
38533|Mabel Creek Ridge paragneisses|69004|6|Mentioned|p18|||Gawler Craton.|||||Paragneisses.|
38533|Mabel Creek Ridge paragneisses|69649|6|Mentioned|p6 Fig.4||||||||Includes paragneisses.|23-FEB-15
22244|Malabena Sandstone Member|24465|5|Briefly described|p353|Early Cambrian|Early Cambrian|Equivalent to the Cooalinga Member.||||||01-SEP-10
22244|Malabena Sandstone Member|60712|4|Described|p35, p30 Fig. 3|Early Cambrian|Early Cambrian|Of Karinya Shale (Silverton Gp). Marker bed.||||||
22244|Malabena Sandstone Member|61307|5|Briefly described|p6 Fig. 3, p7|Cambrian|Cambrian|Of the Karinya Shale (Kanmantoo Group). Geological Province: Karinya Syncline/Adelaide Fold Belt.||||||
25196|Malabine Coal|13497|6|Mentioned|p89, p204|||Informal name for the most laterally extensive coal unit within the Patchawarra Formation. Up to 30m thick. ||Patchawarra Formation||||
25196|Malabine Coal|41595|5|Briefly described|p30|||Reserved as Malabine||||||
74644|Malbooma Granite|40644|6|Mentioned|p132, p133 Fig. 17|Paleoproterozoic|Paleoproterozoic|Name is probably not intended to be formal. Age: ca. 1701+/-30Ma Rb/Sr. Granitic gneiss rocks.||||||29-NOV-19
81752|Malbooma Supersuite|67323|6|Mentioned|Eastern Australia Time-Space Plot|||Southern Gawler Craton.||||||
81618|Mallabie Basalt|72344|5|Briefly described|p7, p11|Stenian|Stenian|Coompana Province. Intersected in drillholes Mallabie 1, CDP002, CDP003, CDP006, CDP008, CD1 and KN2. See also Mallabie Volcanics p3.|c. 1074 Ma|Giants Head Suite, Warakurna Supersuite|||Olivine dolerite gabbro plutons, quenched basalt dykes and vesicular olivine basalt.|04-SEP-19
81618|Mallabie Basalt|72947|2|Defined|p7-9, p11, p14, p19-21|Stenian|Stenian|Coompana Province, eastern. Named after Mallabie Tank. No known surface exposures. Type locality: CDP008 (drillhole 299062, interval 582.80-652.65 m). Carbonate, sericite and hematite alteration is common. Similar geochemistry and the same remnant magnetic signature as the intrusions of the Giants Head Suite; thus, interpreted as coeval. Unit is preserved in two main areas; an irregular area with lobate margins that extends westwards from near Mallabie 1 for 100 km, and northwards from the coast for ~100 km, and a smaller north-south aligned elliptical area (~10 by 5 km) of basalt flows. Maximum thickness: 289.56 m. Drill logs report 2 to 20 m thick lava flows.|c. 1074 Ma|Giants Head Suite, Warakurna Supersuite||Overlies Koomalboogurra Suite. Overlies a sequence of reddish brown, medium-grained to granular arkosic sandstone, with a maximum depositional age of c. 1151 Ma.|Dominantly dark brown-green, massive, fine/medium-grained and variably vesicular to amygdaloidal basalts with brecciated basalts (very fine grained, hematite-rich, siltstone matrix) and minor epiclastic, fine-grained, laminated volcaniclastic rocks.|29-NOV-22
81618|Mallabie Basalt|73224|6|Mentioned|p42|||||Warakurna Supersuite||||
81618|Mallabie Basalt|73225|5|Briefly described|p4||||c.1074 Ma.|Warakurna Supersuite.||||
81618|Mallabie Basalt|73641|6|Mentioned|p2, 4, 13|||||Giants Head Suite||Fed by Giants Head Suite.||
23756|Mambray Formation|40942|6|Mentioned|p21|||||||||
23756|Mambray Formation|40976|6|Mentioned|Table 1|||||||||
23756|Mambray Formation|41292|6|Mentioned|p52|||||||||
23756|Mambray Formation|42475|6|Mentioned|p24|||||||||
23756|Mambray Formation|44133|5|Briefly described|p220 Fig. 11.2|Pleistocene|Pleistocene|||||||
23756|Mambray Formation|62577|6|Mentioned|p566|Late Pleistocene|Late Pleistocene|||||||
23756|Mambray Formation|70334|4|Described|p3,61-63,66,70,83|Late Pleistocene|Late Pleistocene|Of Spencer Gulf area. Thickness: 15cm to 3.5m on CULTANA. Transgressive marine unit, terminated by marine regression, sub-aerial exposire and pedogenesis. Characterised by paleosol development at its top with weakly clay-enriched horizon over a calcareous horizon. Occurs extensively beneath the floor of the Spencer Gulf. Deposited in open estuarine and seagrass bank environments, intertidal and supratidal facies (Hails et al 1984). Contains Late Pleistocene bivalve Anadara trapezia and foraminifer Marginopora vertebralis fossils. Inferred to have been deposited ~125kya during the last interglacial.||||Overlain by False Bay Formation. Disconformably overlain by the Saint Kilda Formation. Underlain by Hindmarsh Clay. Equivalent to Glanville Formation.|Mottled shelly clays to moderately cemented skeletal calcarenites and coquinas, and contains fossils of bivalves, gastropods and benthic foraminifers.|14-OCT-19
67962|Mangatitja Formation|44133|5|Briefly described|p186, 180 Fig. 10.22|Pleistocene|Pliocene|Geological Province: Eucla Basin. Formerly Mangatitja Limestone. Thickness: 30m. Uncoformably overlies probable Garford Formation.|||||Limestone, alluvial redbed facies including sand, grit, flood-plain to fan clay.|04-DEC-13
67962|Mangatitja Formation|67462|5|Briefly described|Map legend.|Pliocene|Miocene|Serpentine Lakes-Lindsay and Stevenson-Mirackina Regions.||||||
67962|Mangatitja Formation|67921|6|Mentioned|Map legend|Pliocene|Miocene|||||Equivalent to Garford Formation||
67962|Mangatitja Formation|68715|6|Mentioned|p30 Fig.5|Piacenzian|Langhian|Serpentine Lakes-Lindsay Region.||||||
67962|Mangatitja Formation|71416|5|Briefly described|Map legend.|Pleistocene|Miocene||||||Olive-green, calcareous sandy clay. May contain red-clayey saprolite or polished silcrete pebbles.|
67962|Mangatitja Formation|73090|5|Briefly described|p12 Fig.7, Appendix|Pliocene|Miocene||||||Limestone, red bed facies, sand, grit, and flood-plain to fan clay. Palaeochannel fill.|
67962|Mangatitja Formation|73100|5|Briefly described|Map legend|Pliocene|Miocene|||||Equivalent to Garford Formation.||
67962|Mangatitja Formation|73109|5|Briefly described|Map legend.|Pliocene|Miocene|||||Equivalent to Garford Formation.||
67962|Mangatitja Formation|73111|5|Briefly described|Map legend.|Pliocene|Miocene|||||Equivalent to Garford Formation.||
67962|Mangatitja Formation|73232|6|Mentioned|p8|||Lacustrine palaeovalley infill. One of the main stratigraphic units in palaeovalleys that trend southwards from the Musgrave Province across the Officer Basin to the Eucla Basin.||||||
80276|Manguri Group|71341|5|Briefly described|p196, p199|Palaeoproterozoic|Palaeoproterozoic|Northern Gawler Craton. An informal group of meta-sedimentary rocks found in the Nawa Domain, Mount Woods Inlier, Peake and Denison Block, Mabel Creek Ridge, Welboum Hill and Yoolperlunna regions. Named for the Manguri region of South Australia. |ca. 1740 Ma||||Metasedimentary rocks.|23-OCT-17
80276|Manguri Group|73525|6|Mentioned|p18|||Gawler Craton, northern (buried). Correlated with Leichhardt Superbasin.||||||
41895|Maralinga Member|61234|4|Described|p6, p7 Fig 4.|Middle Eocene|Middle Eocene|Of the Pidinga Formation. Overlain by Anthony Member. Geological Province: Eucla Basin. Fluvial carbonaceous clastics.||||||08-FEB-10
41895|Maralinga Member|61856|5|Briefly described|p300 Fig.2, p304, p311-313  |Middle Eocene|Middle Eocene|Revised name after Clarke et al. (2003). Marginal marine-fluvial deposits. Basal Tertiary unit in eastern Eucla Basin.||Of the Pidinga Formation||Overlain gradationally by Paling Limestone or Anthony Member.|Upward-fining cycles capped by carbonaceous mud.|
41895|Maralinga Member|64646|6|Mentioned|p23 Fig. 3|Oligocene|Eocene|Of Pidinga Formation. Geological Province: Gawler Craton.||||||08-FEB-10
41895|Maralinga Member|67462|5|Briefly described|Map legend.|Eocene|Eocene|Eucla Basin.||Unit in Pidinga Formation.||Is overlain by Anthony Member.||
41895|Maralinga Member|68715|6|Mentioned|p30 Fig.5|Bartonian|Ypresian|SW and NW Gawler Craton, Eucla Basin.||Pidinga Formation.||||07-APR-17
41895|Maralinga Member|69598|6|Mentioned|p9|Middle Eocene|Middle Eocene|||||||
34361|Marino Arkose Member|22510|5|Briefly described|p39, table1|||Basal arkose member of the Wilmington Formation.  Formerly Marino Arkose.  Type section unchanged. Age: Marinoan. Adelaide region||||||26-NOV-22
34361|Marino Arkose Member|61732|5|Briefly described|p4 Fig. 3, p28 Fig. 13|Marinoan|Sturtian|Of the Wilmington Formation (Upalinna Subgroup, Umberatana Group).  Age: 657+/-17Ma. Geological Province: Adelaide Rift Complex/Stuart Shelf.||||||07-FEB-11
34361|Marino Arkose Member|62453|4|Described|p12 Fig. 8|Ediacaran|Cryogenian|Geological Province: Adeliade Rift Complex/Stuart Shelf. Age: 657 +/- 17Ma. Of the Umberatana Group.||||||
34361|Marino Arkose Member|65365|5|Briefly described|p10 Fig. 4|||Within Umberatana Group. ?detrital zircon grain dated 657 +/- 17 Ma (Preiss, 2000).||||||19-MAR-12
34361|Marino Arkose Member|65366|5|Briefly described|p23 Fig. 3|Ediacaran|Ediacaran|Within Umberatana Group. ?detrital zircon grain  dated 657 +/- 17 Ma (Preiss, 2000).||||||19-MAR-12
34361|Marino Arkose Member|68269|6|Mentioned|p674|Cryogenian|Cryogenian|Age is U-Pb detrital zircon age.|657 +/- 17 Ma|Upalinna Subgroup||||
34361|Marino Arkose Member|68270|5|Briefly described|p683|Cryogenian|Cryogenian|Adelaide Rift Complex. 657+\-17 Ma maximum depositional age (detrital zircon), Marino Arkose Member (Ireland et al. 1998).||Unit of Umberatana Group.||||
34361|Marino Arkose Member|70031|5|Briefly described|p246|Cryogenian|Cryogenian|Adelaide Geosyncline. Contains two detrital zircons with poorly defined U-Pb ages of ca. 655 and 650 Ma (Fanning and Link 2008).||Unit of Wilmington Formation.||||
34361|Marino Arkose Member|70082|5|Briefly described|p2-3|Cryogenian|Cryogenian|Kulpara-Adelaide region.||Unit of Wilmington Formation.||Overlain by Reynella Siltstone Member.||
34361|Marino Arkose Member|70382|6|Mentioned|p34|Neoproterozoic|Neoproterozoic|Of Adelaide Rift Complex.||||||
34361|Marino Arkose Member|73188|6|Mentioned|p331|||||||||
34361|Marino Arkose Member|73234|6|Mentioned|p20|Cryogenian|Cryogenian|Age is a single detrital zircon age; Ireland et al. (1998).|657 +/- 17 Ma [see comments]|Umberatana Group||||
34361|Marino Arkose Member|73236|4|Described|p35-38, p41-42, p47|Cryogenian|Cryogenian|Shallow marine sedimentary rocks. Exposed in the south bank of Waterfall Creek east of the railway line at Hallett Cove.|c. 645-640 Ma|Wilmington Formation, Upalinna Subgroup, Umberatana Group, Heysen Supergroup||Underlain by Angepena Formation.|Coarse-grained, calcareous-cemented feldspathic grit with large rounded red feldspar grains up to 5 mm across and ripple-marked siltstone with thin interbeds of limestone and sandy limestone.|
34361|Marino Arkose Member|74367|5|Briefly described|p8-9, p17, p20, p22|Cryogenian|Cryogenian|Misspelt Arkose member p17.|654+/-13 Ma MDA|Wilmington Formation, Upalinna Subgroup||||
28212|Marla Group|22901|6|Mentioned|76 fig 2|||Geol province Officer Basin||||||
28212|Marla Group|22922|5|Briefly described|34|||||||||
28212|Marla Group|23282|4|Described|p68||Neoproterozoic|Was 'Marla Sequence' of Krieg (1973) and defined as Marla Group by Benbow (1982).||||||24-SEP-08
28212|Marla Group|23288|6|Mentioned|Fig.5||Early Cambrian|||||||
28212|Marla Group|23479|5|Briefly described|p26|Paleozoic|Paleozoic|Geological Province: Gawler Craton [??more likely overlies].||||||04-NOV-10
28212|Marla Group|23557|5|Briefly described|p95 Fig.1|Neoproterozoic III|Neoproterozoic III|Geological Province: Officer Basin.||||||
28212|Marla Group|24112|5|Briefly described|p254 Fig.2|Middle Cambrian|Early Cambrian|Geological Province: Officer Basin||||||
28212|Marla Group|38329|2|Defined|p194|Cambrian|Cambrian|||||||
28212|Marla Group|40642|6|Mentioned|p175|||||||||
28212|Marla Group|40945|6|Mentioned|Fig.3|||||||||
28212|Marla Group|42065|5|Briefly described|p185|||See also Fig.2||||||
28212|Marla Group|42357|5|Briefly described|p10|||||||||
28212|Marla Group|43052|5|Briefly described|Fig.2.10|||||||||
28212|Marla Group|43053|5|Briefly described|Map Legend|Cambrian|Cambrian|Includes Wirrildar beds, Trainor Hill Sandstone, Mount Johns Conglomerate, Arcoeillinna Sandstone, Observatory Hill Formation and Wallatinna Formation.||||||
28212|Marla Group|43657|6|Mentioned|Fig.3,p4||Cambrian|||||||
28212|Marla Group|43690|6|Mentioned|Fig.2,p157||Cambrian|||||||
28212|Marla Group|43743|6|Mentioned|Fig.2,p33|Middle Cambrian|Early Cambrian|||||||
28212|Marla Group|44109|5|Briefly described|p22 Fig. 19|Cambrian|Cambrian|Includes the Relief Sandstone, Ouldburra, Observatory Hill and Wallatinna Formations, Arceollinna Sandstone, Mount Johns Conglomerate and Trainor Hill Sandstone. Geological Province: central Officer Basin.||||||
28212|Marla Group|44133|5|Briefly described|p35|||Includes the Refief Sandstone and the Ouldburra Formation.||||||
28212|Marla Group|60565|6|Mentioned|p18|Cambrian|Cambrian|||||||
28212|Marla Group|61732|5|Briefly described|p4 Fig. 3, p67-68|Cambrian|Marinoan|Includes the Relief Sandstone and Ouldburra and Observatory Hill Formations. Unconformably overlies Narana Formation and its Mena Mudstone member. Geological Province: eastern Officer Basin. See also p58 Fig. 22, p89.||||||17-APR-13
28212|Marla Group|62453|5|Briefly described|p5 Fig. 3|Cambrian|Cambrian|Geological Province: Officer Basin.||||||
28212|Marla Group|62570|5|Briefly described|p579, p580 Figs. 2 and 3|Middle Cambrian|Early Cambrian|Includes Relief Sst, Ouldburra and Observatory Hill Fm, Arcoeillinna and Trainor Hill Ssts. Thickness: >1.5km. Type section in Manya Trough area. Unconformable over Ungoolya Gp. Contains mainly siliciclastics with some carbonates. Geol.prov: Officer Basin||||||10-AUG-07
28212|Marla Group|63224|5|Briefly described|p8|Cambrian|Cambrian|Informally divided into upper and lower Marla Group on the basis of drillhole stratigraphy.||||||02-MAY-07
28212|Marla Group|64103|6|Mentioned|p400 Fig. 3|Cambrian|Cambrian|Geological Province: Officer Basin.||||||07-FEB-11
28212|Marla Group|64794|6|Mentioned|p240 Tb.1|Middle Cambrian|Early Cambrian|Officer Basin. 900m thick.||||||
28212|Marla Group|64970|6|Mentioned|p719 Fig. 2|Cambrian|Neoproterozoic|Geological Province: Officer Basin.||||||27-MAY-09
28212|Marla Group|65313|5|Briefly described|p578, Fig 6|Ordovician|Cambrian|Officer Basin. Ungoolya 1 well.|||Includes Observatory Hill Formation, Apamurra Formation, Trainor Hill Sandstone.|Underlies Munda Group.||26-MAR-12
28212|Marla Group|65365|5|Briefly described|p10 Fig. 4|Ediacaran|Ediacaran|Eastern Officer Basin. Includes Ediacara fauna.||||||19-MAR-12
28212|Marla Group|65366|5|Briefly described|p23 Fig. 3|Ediacaran|Ediacaran|Eastern Officer Basin. Includes Ediacara fauna||||||
28212|Marla Group|65376|5|Briefly described|p9 Fig.1.2. |Paleozoic|Paleozoic||||||Evaporitic fluvial, eolian and marine sediments.|
28212|Marla Group|67120|5|Briefly described|Map legend|Cambrian|Cambrian||||Includes Apamurra Formation, Arcoeillinna Sandstone, Observatory Hill Formation, Relief Sandstone, Trainor Hill Sandstone.||Sandstone, limestone, evaporites.|
28212|Marla Group|68131|5|Briefly described|p2 Fig.1|Cambrian|Cambrian|Evaporitic fluvial, aeolian and marine sediments.||||||
28212|Marla Group|69003|6|Mentioned|p60|Cambrian|Cambrian|E Officer Basin.||||||
28212|Marla Group|69648|4|Described|p19, p34-35, map legend|Middle Cambrian|Early Cambrian|Early to Middle Cambrian sediments of Tallaringa Trough (Relief Sandstone, Ouldburra Formation) may extend into northeastern OOLDEA.|Minimum: ~507 Ma||Relief Sandstone, Ouldburra Formation|||
28212|Marla Group|70336|5|Briefly described|Map legend|Cambrian|Cambrian||||Includes Trainor Hill, Relief, Arcoeillinna Sandstones; Apamurra, Observatory Hill Formations.||Sandstone, limestone, evaporites.|12-JAN-16
28212|Marla Group|71146|5|Briefly described|p6|Cambrian|Cambrian|Officer Basin.||||Overlain by the Table Hill Volcanics.|Sandstone, mudstone and evaporite.|
28212|Marla Group|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone|
28212|Marla Group|71268|5|Briefly described|1m_geologyp12_lut.csv||||||Includes Wirrildar beds.|||
28212|Marla Group|72476|5|Briefly described|p26, 35, p36 Fig.9|||Officer Basin. Sediments derived from the Musgrave Block. Early Paleozoic.|||||Clastic sedimentary rocks.|
28212|Marla Group|72478|5|Briefly described|p8, p9|Middle Cambrian|Early Cambrian|Officer Basin.|c. 545 Ma-510 Ma||Includes the Ouldburra Formation, Relief Sandstone, Observatory Hill Formation, Arcoeillinna Sandstone, Apamurra Formation, Trainor Hill Sandstone.|||25-MAR-21
28212|Marla Group|73090|5|Briefly described|p12 Fig.7|Cambrian|Cambrian||||Observatory Hill Formation, Trainor Hill Sandstone.|||
28212|Marla Group|73099|5|Briefly described|Map legend.|Middle Cambrian|Early Cambrian|Officer Basin.|||Relief, Arcoeillinna, Trainor Hill Sandstones; Observatory Hill, Apamurra Formations.|Overlies Ungoolya Group. Is overlain by Munda Group.||
33661|Marne River Volcanics|22945|5|Briefly described|p8|||Mentioned under - Area C geology.||||||
33661|Marne River Volcanics|23731|6|Mentioned|p43|||||||||
33661|Marne River Volcanics|24509|5|Briefly described|p42, p39 Fig. 1|Cambrian|Cambrian|Alkaline volcanics. Deposited as tuffs. Age: ~521Ma. Geological Province: Murray Basin.||||||04-MAY-05
33661|Marne River Volcanics|60567|2|Defined|p37|Early Cambrian|Early Cambrian|Originally interpreted as part of Kanmantoo Group. Various lithologies show metamorphic recrystallisation. More felsic than Teal Flat Volcanics consisting of calc-alkaline dacite, rhyodacite to rhyolite volcanics to volcaniclastics. Age: 521+/-4Ma.||||||19-NOV-04
33661|Marne River Volcanics|67536|5|Briefly described|Map Legend|||Kanmantoo Province; basement to Murray Basin.|ca. 521 +/- 4 Ma - 478 +/- 23 Ma|||Intercalated with Kanmantoo Group metasediments|Felsic-intermediate volcanic rocks.|
33661|Marne River Volcanics|71322|5|Briefly described|p52 Fig.1, p71-74|Cambrian|Cambrian|Geochemical plots. Elevated REE in this unit probably reflects a more crustal source region. U-Pb SHRIMP geochronology used.|521 +/- 4 Ma (Burtt et al., 2000).|Normanville Group.||Intercalated with Normanville and/or Kanmantoo Group. Provisionally correlated with Truro Volcanics.|Felsic-intermediate volcanics: metamorphically recrystallised interlayered volcanics, volcaniclastics, intrusives and sediments.|14-DEC-21
33661|Marne River Volcanics|73093|5|Briefly described|map legend|Cambrian|Cambrian||||||Quartzo-feldspathic tuffaceous rhyolitic-dacitic volcaniclastics inter-laytered with metasandstone, metasiltstone and calc-silicate rock.|09-DEC-21
33661|Marne River Volcanics|73188|6|Mentioned|p342|Cambrian|Cambrian|||||||
34759|Marola Sandstone Member|22889|2|Defined|p34-35 & p 39|Adelaidean|Adelaidean|Situated in the western belt of the Skillogalee Dolomite occuppying the Gladstone Trough, between the Torrens Hinge Zone and the Clare-Spalding Fault.||||||
75586|Marsden Sandstone|66761|2|Defined|p256 App 1, p245 Fig.2, 247-250, 252-254|Early Cambrian|Early Cambrian|New Name. 43m in type section. Age: Cambrian Series 2 Stage 4|||Includes Rouge Mudstone Member.|Conformably overlies White Point Conglomerate. Unconformably overlain by Emu Bay Shale.|Mudstone at base with calcareous feldspathic sandstone above, mudstone and sandstone then coarsening upward to gravel conglomerate towards the top.|14-MAR-12
75586|Marsden Sandstone|67344|4|Described|p260 Fig.1, p261|Early Cambrian|Early Cambrian|The upper part of White Point Conglomerate has been redefined as the Marsden Sandstone (defined by Gehling et al. 2011). Lower Cambrian age. ~ 43m thick in its type section.|||Includes the Rouge Mudstone Member.|Conformably overlies White Point Conglomerate. Overlain by the Emu Bay Shale.|Bioturbated calcareous mudstone; coarsening-upward, slightly calcareous, feldspathic sandstone with subordinate mudstone and gravel.|17-SEP-14
75586|Marsden Sandstone|73247|5|Briefly described|p204-207, p209-210|||Part of the eastern succession of the Kangaroo Island Group. Established by Gehling et al. (2011). Previously considered a finer-grained upper part of the White Point Conglomerate. Fossil evidence is used to correlate the unit with the Smith Bay Shale from the western succession.||Kangaroo Island Group|Rouge Mudstone Member|Underlain by White Point Conglomerate. Unconformably overlain by Emu Bay Shale. Correlates to Smith Bay Shale. Equivalent to Kanmantoo Group.||02-FEB-23
27190|Maslin Sands|22525|4|Described|p35,37|Oligocene|Eocene|Combination of North and South Maslin Sands.||||||12-NOV-08
27190|Maslin Sands|30250|6|Mentioned|Table 2|||See also Table 3.||||||
27190|Maslin Sands|35689|2|Defined|p12|Eocene|Eocene|||||||
27190|Maslin Sands|35697|6|Mentioned|p90|||||||||
27190|Maslin Sands|36127|5|Briefly described|p9|||See also P7.||||||
27190|Maslin Sands|36244|6|Mentioned|p2|||Redefined by Cooper 1979.||||||
27190|Maslin Sands|38621|6|Mentioned|Table 1|||Refers Cooper 1979.||||||
27190|Maslin Sands|38622|6|Mentioned|p8|||||||||
27190|Maslin Sands|39351|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
27190|Maslin Sands|39929|6|Mentioned|p283|||||||||
27190|Maslin Sands|40442|4|Described|p25|||||||||
27190|Maslin Sands|40778|6|Mentioned|p534|||||||||
27190|Maslin Sands|40969|6|Mentioned|Fig.1|||||||||
27190|Maslin Sands|41513|6|Mentioned|p45|||Mention Fig.4||||||
27190|Maslin Sands|61155|5|Briefly described|p3, p17|Middle Eocene|Middle Eocene|Fluvial to paralic sands. Overlain by Tortachilla Limestone. Age: 49.5-40Ma. Max. thickness: 80m.||||||
27190|Maslin Sands|64397|5|Briefly described|p232 Fig. 1A|Eocene|Eocene|Probably an informal compound term for North Maslin and South Maslin Sands. Geological province: St Vincent Basin.||||||
27190|Maslin Sands|68811|5|Briefly described|p87, p88, p128 tbl 15, p154 app 1|Tertiary|Tertiary|||||Overlain by the Blanch[e] Point Formation and the Port Willunga Formation.|Fine to coarse sands and clays.|15-APR-20
38347|Massena Bay Gneiss|23791|6|Mentioned|p5 Fig. 4|||||||||
38347|Massena Bay Gneiss|50605|5|Briefly described|p3.2|||Intruded by Donington Granitoid Suite. Geological Province: Gawler Craton & Curnamona Province.||||||
38347|Massena Bay Gneiss|61307|5|Briefly described|p39 Fig. 19|||See also Massena Bay Gneisses. Age: <2600Ma. Geological Province: Gawler Craton.||||||
39165|Matta Formation|24475|2|Defined|p55|Paleoproterozoic|Paleoproterozoic|Of Wallaroo Group.||||||07-NOV-08
39165|Matta Formation|60958|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Wallaroo Group. Mafic volcanics and intrusives. Intrudes both the Wandearah and Weetulta Formations. Geological Province: Gawler Craton.||||||07-NOV-08
39165|Matta Formation|61121|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|All mafic volcanics or intrusives in the Wallaroo Formation. Intrudes both Wandearah and Weetulta Formations. Geological Province: Gawler Craton.||||||07-NOV-08
39165|Matta Formation|65375|5|Briefly described|p19, p23.|||Includes all mafic rocks associated with Wallaroo Group.||Unit in Wallaroo Group.|Comprises Willamulka Volcanics Member and Renowden Metabasalt Member.||Metabasalt, metadolerite, amphibolites.|
39165|Matta Formation|65376|6|Mentioned|p101. |||||Unit in Wallaroo Group.||||
39165|Matta Formation|66302|5|Briefly described|p29|||||Wallaroo Group|||Mafic volcanic rocks including tholeiites.|
39165|Matta Formation|68131|6|Mentioned|p7, p17|Paleoproterozoic|Paleoproterozoic|Yorke Peninsula.||||||
39165|Matta Formation|71129|6|Mentioned|p39|Statherian|Statherian|Geological Province: Gawler Craton. Deposition synchronous with Wandearah Formation.||||||
39165|Matta Formation|71799|5|Briefly described|p150 fig 2|Statherian|Statherian|Eastern Gawler Craton.|ca 1750 Ma|Wallaroo Group||Overlies the Moonta and Mona formations.|Basalt, dolerite, gabbro or amphibolite.|
39165|Matta Formation|73165|6|Mentioned|p621|||Gawler Craton, Moonta Domain, northern Yorke Peninsula.|||||Includes intrusives.|
23777|McGregor Volcanics|22613|6|Mentioned|p29|||||||||
23777|McGregor Volcanics|22629|5|Briefly described|p152, figs2,4|Statherian|Statherian|Age: 1740Ma from U-Pb dating.||||||18-JAN-07
23777|McGregor Volcanics|23054|6|Mentioned|p9||Statherian|Max Age: ~1740 Ma.||||||
23777|McGregor Volcanics|23481|5|Briefly described|p19 Fig 1|||Geological Province: Gawler Craton.||||||
23777|McGregor Volcanics|23719|4|Described|p17|Statherian|Statherian|See also page 14 table 1. Age: ~1740 Ma (U-Pb zircon). Previously known as Moonabie Volcanics and/or Moonabie Porphyry. Overlain by Moonabie Formation. Underlain by Broadview Schist. Geological Province: Gawler Craton. Max. thickness: >1000 m.||||||18-JAN-07
23777|McGregor Volcanics|23805|5|Briefly described|p4 Fig. 1|Paleoproterozoic|Paleoproterozoic|Geological Province: Gawler Craton.||||||07-NOV-08
23777|McGregor Volcanics|24197|5|Briefly described|p74 Tb. 8.1|Paleoproterozoic|Paleoproterozoic|Age: 1750-1700Ma.||||||07-FEB-11
23777|McGregor Volcanics|24475|5|Briefly described|p50|Statherian|Statherian|Age: ~1740 Ma (SHRIMP U-Pb).||||||
23777|McGregor Volcanics|24505|5|Briefly described|p5 Fig. 1|||Geological Province: Gawler Craton.||||||
23777|McGregor Volcanics|24526|6|Mentioned|p99|Paleoproterozoic|Paleoproterozoic|Age: 1740Ma.||||||07-NOV-08
23777|McGregor Volcanics|37811|6|Mentioned|Fig.2|||||||||
23777|McGregor Volcanics|39344|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
23777|McGregor Volcanics|39349|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
23777|McGregor Volcanics|39488|6|Mentioned|p2|||||||||
23777|McGregor Volcanics|39802|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
23777|McGregor Volcanics|40448|5|Briefly described|p36|||||||||
23777|McGregor Volcanics|40644|6|Mentioned|p120 Fig. 2, p121|Paleoproterozoic|Paleoproterozoic|Formerly "Moonabie Porphyry" and "Moonabie Volcanics". Age: 1645+/-15Ma and 1615+/-29Ma (see Table 4, p135) - latter age is preferred.  See also p124 Fig. 3.||||||02-JUN-09
23777|McGregor Volcanics|41239|6|Mentioned|p95|||||||||
23777|McGregor Volcanics|41325|6|Mentioned|p18|||||||||
23777|McGregor Volcanics|41402|6|Mentioned|p35|||||||||
23777|McGregor Volcanics|41493|6|Mentioned|Table 1|||||||||
23777|McGregor Volcanics|41609|6|Mentioned|Fig.1|||||||||
23777|McGregor Volcanics|41667|4|Described|p70|||Briefly described p6.||||||18-JAN-07
23777|McGregor Volcanics|41972|4|Described|p377|||||||||
23777|McGregor Volcanics|42469|6|Mentioned|p13|||Port Augusta, SI53-4||||||
23777|McGregor Volcanics|42934|5|Briefly described|p520|||Intruded by Charleston Granite.||||||12-JAN-10
23777|McGregor Volcanics|43052|4|Described|p66|||Age about 1740 Ma.||||||18-JAN-07
23777|McGregor Volcanics|43053|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Acid and basic volcanics.||||||07-NOV-08
23777|McGregor Volcanics|43141|6|Mentioned|p63,Fig.1|||||||||
23777|McGregor Volcanics|43258|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
23777|McGregor Volcanics|43298|6|Mentioned|Map Legend||Paleoproterozoic|||||||07-NOV-08
23777|McGregor Volcanics|50605|5|Briefly described|p(i), 1.3, 5.1, 8.6, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Gawler Craton and Curnamona Province. Age: 1755-1740 +/- 12Ma (U-Pb). Of the Younger Lincoln Supersuite. Intruded by Hiltaba Supersuite.||||||07-NOV-08
23777|McGregor Volcanics|60515|6|Mentioned|p116 Fig.1 |||||||||
23777|McGregor Volcanics|60953|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Age: ~1740Ma. Rhyolite to dacite, minor andesite and basalt.||||||07-NOV-08
23777|McGregor Volcanics|60954|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Geological Province: Gawler Craton.||||||07-NOV-08
23777|McGregor Volcanics|61108|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|Rhyolite to dacite, minor andesite and basalt. Age: ~1740 Ma.||||||07-NOV-08
23777|McGregor Volcanics|61262|5|Briefly described|p455 Fig. 11|Paleoproterozoic|Paleoproterozoic|Age: >1750Ma. Geological Province: eastern Gawler Craton.||||||07-NOV-08
23777|McGregor Volcanics|61307|5|Briefly described|p36 Fig. 17|Paleoproterozoic|Paleoproterozoic|Geological Province: Gawler Craton. See also p39 Fig. 19.||||||07-NOV-08
23777|McGregor Volcanics|61522|5|Briefly described|p5 Fig.1|||Geological Province: Gawler Craton.||||||
23777|McGregor Volcanics|62893|6|Mentioned|p12|Palaeoproterozoic|Palaeoproterozoic|Gawler Craton.||||||
23777|McGregor Volcanics|63020|5|Briefly described|p987 Fig. 8|Paleoproterozoic|Paleoproterozoic|Age: ~1740Ma. Geological Province: Gawler Craton (Spencer Domain).||||||07-NOV-08
23777|McGregor Volcanics|63866|5|Briefly described|p6, p9, p31|||Spencer Domain, Gawler Craton.||||||
23777|McGregor Volcanics|64130|5|Briefly described| p1380 Fig.2, p1381|||Eastern Gawler Craton.|ca. 1740 Ma (Fanning et al., 1988).|||||
23777|McGregor Volcanics|64313|5|Briefly described|p450 Fig. 1|Paleoproterozoic|Paleoproterozoic|Age: ~1740Ma. Geological province: Gawler Craton. See also p451 Fig.2b.||||||09-FEB-10
23777|McGregor Volcanics|64722|6|Mentioned|Fig. 5 p13|Paleoproterozoic|Paleoproterozoic|Of South Australian Craton.||||||
23777|McGregor Volcanics|64725|6|Mentioned|p58 Fig.2. |||Gawler Craton.||||||
23777|McGregor Volcanics|64739|6|Mentioned|p264 Fig.1. |Paleoproterozoic|Paleoproterozoic|Gawler Craton.||||||
23777|McGregor Volcanics|65221|5|Briefly described|p26|Palaeoproterozoic|Palaeoproterozoic|1745Ma, Cleve Domain. Intruded by Gawler Range Volcanics and Hiltaba Suite.||||||10-MAR-10
23777|McGregor Volcanics|65375|6|Mentioned|p19.|||Northern Eyre Peninsula.||||||
23777|McGregor Volcanics|65376|5|Briefly described|p8 Fig.1.1, pp108-109, p235.|||Eyre Peninsula. May be equivalent to volcanics in Spring Hill area.|c.1745 Ma.|||||
23777|McGregor Volcanics|65390|5|Briefly described|p23 Fig.3, p26 Tb. 1|Statherian|Statherian|Spencer Domain, Gawler Craton. Underlies Moonabie Formation, overlies Broadview Schist. Intruded by Charleston Granite of Hiltaba Suite. Age of 1740 Ma in Figure 3.||||||
23777|McGregor Volcanics|65483|4|Described|p19|Palaeoproterozoic|Palaeoproterozoic|Underlies and intertongues with Moonabie Formation. Bimodal acidic and lesser mafic volcanics. Age: c 1740 Ma  (Fanning et al. 1988).||||||04-MAR-13
23777|McGregor Volcanics|65772|6|Mentioned|p229 Fig.2, p234 Fig.8|Statherian|Statherian|1790 Ma||||||
23777|McGregor Volcanics|65915|5|Briefly described|p5|Statherian|Statherian|Sedimentary and volcanic rocks deposited between ~1790-1740 Ma east of Kalinjala Mylonite Zone.||||||
23777|McGregor Volcanics|65922|6|Mentioned|p13 Fig. 4|||Gawler Craton.||||||
23777|McGregor Volcanics|66302|5|Briefly described|p4 Fig.3, p28, p30, p33, p34|Statherian|Statherian|Spencer Domain, Gawler Craton. A-type geochemistry. See also p47, p63, p76 Fig.20. |1754 +/- 5 Ma (SHRIMP Fraser and Neumann, 2010)|||Interlayered with the Moonabie Formation. Unconformably overlain by the Corunna Conglomerate. Intruded by the Charleston Granite.|Porphyritic rhyolite, rhyodacite, dacite and andesite-basalt.|
23777|McGregor Volcanics|67323|5|Briefly described|Eastern Australia Time-Space Plot; p32|||Gawler Craton.|1754 +/- 5 Ma.||||Bimodal volcanics.|
23777|McGregor Volcanics|67536|5|Briefly described|Map Legend|Statherian|Statherian|Gawler Craton.|ca. 1740 Ma||||Rhyolite, dacite, andesite and basalt.|
23777|McGregor Volcanics|67581|6|Mentioned|p45|||Gawler Craton. Pre-Kimban (1790-1740 Ma) Orogeny.||||||
23777|McGregor Volcanics|68158|5|Briefly described|p1-2, p4-6, p8-9, p13, p15-17, p21-22|||Likely protoliths for the Moonabie Formation. Also gives ID-TIMS U-Pb zircon age of c.1750-c.1740 Ma (Fanning, 1998). Sm-Nd values.|1754 +/- 5 Ma (SHRIMP U-Pb zircon).|||Interbedded with Moonabie Formation.||
23777|McGregor Volcanics|68208|6|Mentioned|p32 Fig.3|Paleoproterozoic|Paleoproterozoic|Grouped with Moonabie Formation.||||||
23777|McGregor Volcanics|69004|6|Mentioned|p18|||Gawler Craton.||||||
23777|McGregor Volcanics|69048|6|Mentioned|p3|||Eyre Peninsula / Yorke Peninsula.|c.1775-1750 Ma.|||||
23777|McGregor Volcanics|69649|6|Mentioned|p6 Fig.4|||||||||
23777|McGregor Volcanics|69666|6|Mentioned|p27 Fig.3|Paleoproterozoic|Paleoproterozoic|||||||
23777|McGregor Volcanics|70027|5|Briefly described|p56-57,71|Statherian|Statherian|Geological province: Gawler Craton. Deposited at ca. 1755 Ma just prior to the 1730-1690 Ma Kimban Orogeny. Possible source of ca. 1790-1750 Ma zircons associated with the Warramboo magnetite gneiss.|ca. 1755 Ma|||||
23777|McGregor Volcanics|70334|5|Briefly described|p10,74|Statherian|Statherian|Geological province: Gawler Craton. Bimodal sequence of felsic and minor basaltic volcanics (Parker and Fanning, 1998) which erupted at 1754+\-5 Ma (Fraser and Neumann, 2010). Contemporaneous with Moonabie Formation.|1754+\-5 Ma|||||
23777|McGregor Volcanics|70659|5|Briefly described|p9|Palaeoproterozoic|Palaeoproterozoic|The major source of detritus for the Moonabie Formation.|1754 +/- 5 Ma (Fraser and Neumann, 2010).|||||
23777|McGregor Volcanics|70721|6|Mentioned|p64|Paleoproterozoic|Paleoproterozoic|||||||
23777|McGregor Volcanics|71037|6|Mentioned|p21 Fig.1|Paleoproterozoic|Paleoproterozoic|Shown only on 'Outcropping geology and mineral deposits of northern Eyre Peninsula' map p21 Fig.1.||||Shown as younger than Tip Top Granite and older than Wallaroo Group.||
23777|McGregor Volcanics|71129|5|Briefly described|p14,17-18,31,35-36,44,204|Statherian|Statherian|Geological Province: Olympic Domain, Gawler Craton. Primary source of detrital material in the Moonabie Formation.|c. 1754+\-5 Ma (Fraser and Neumann, 2010)|||Overlain by, and intertongues with Moonabie Formation.||13-NOV-19
23777|McGregor Volcanics|71235|6|Mentioned|p8-p9, p13|Palaeoproterozoic|Palaeoproterozoic||c. 1745 Ma (Fanning et al., 1988).|||||
23777|McGregor Volcanics|71236|5|Briefly described|p5|Statherian|Statherian||c. 1740 Ma (Fanning et al., 1988)|||Overlain by and intertongues with the Moonabie Formation.|Bimodal acidic and lesser mafic volcanics.|
23777|McGregor Volcanics|71317|5|Briefly described|p15-p16|Palaeoproterozoic|Palaeoproterozoic|Olympic Domain, Gawler Craton.|c. 1755 Ma|||||
23777|McGregor Volcanics|71341|6|Mentioned|p194, p196|||Broadly geochemically similar to the Myola Volcanics, Cleve Group, Price Metasediments, Moonabie Foramtion and the Wallaroo Group. |ca. 1750 Mna (Turner et al, 1993)|||||
23777|McGregor Volcanics|71348|6|Mentioned|p201|Statherian|Statherian|Geological province: Gawler Craton.||||||
23777|McGregor Volcanics|71413|6|Mentioned|p32 Fig 2|||Geological province: Gawler Craton. ||||||
23777|McGregor Volcanics|71534|6|Mentioned|p296|Statherian|Statherian|Geological province: Gawler Craton.||||||
23777|McGregor Volcanics|71559|6|Mentioned|p15 Fig 1|Paleoproterozoic|Paleoproterozoic|Geological province: Gawler Craton.||||||
23777|McGregor Volcanics|71859|5|Briefly described|p3-p4, p6|Paleoproterozoic|Paleoproterozoic|Olympic Domain, southern Gawler Craton.|1755 Ma|||||
23777|McGregor Volcanics|71862|6|Mentioned|p3|||||||||
23777|McGregor Volcanics|72058|6|Mentioned|p171|||Middleback Ranges, Gawler Craton.|1754-1740 Ma|||||
23777|McGregor Volcanics|72090|6|Mentioned|p10|Statherian|Statherian|Olympic Domain, Gawler Craton.|c. 1755 Ma|||||
23777|McGregor Volcanics|72459|6|Mentioned|p51|Palaeoproterozoic|Palaeoproterozoic|Lincoln Domain.|c. 1740 Ma|||||
23777|McGregor Volcanics|72462|6|Mentioned|p3, p10|Statherian|Statherian|Gawler Craton.|1754 +/- 5 Ma|||||
23777|McGregor Volcanics|72463|6|Mentioned|p2|Paleoproterozoic|Paleoproterozoic|||||||
23777|McGregor Volcanics|72484|6|Mentioned|p3|||Eyre Peninsula, Gawler Craton.|~1754-1740 Ma.|||||
23777|McGregor Volcanics|72949|6|Mentioned|p33, p37|Statherian|Statherian|Emplaced prior to Kimban Orogeny. Crustal Nd isotopic compositions/signatures. eNd(1740 Ma) = -3.4 to -0.6 (Turner et al., 1993).|c. 1740 Ma|||||
23777|McGregor Volcanics|73026|5|Briefly described|p6, p9|Paleoproterozoic|Paleoproterozoic|Eyre Peninsula/Yorke Peninsula.|c. 1750 Ma||||Mafic volcanics.|
23777|McGregor Volcanics|73027|6|Mentioned|p6, p9|||Eastern Eyre Peninsula/Yorke Peninsula.|c. 1750 Ma|||||
23777|McGregor Volcanics|73030|6|Mentioned|p2149|Statherian|Statherian|Gawler Craton.||||||
23777|McGregor Volcanics|73103|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic||||||Volcanics, bimodal, acidic and lesser basaltic volcanics.|
23777|McGregor Volcanics|73110|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic||||||Volcanics, bimodal, acidic and lesser basaltic volcanics.|
23777|McGregor Volcanics|73130|6|Mentioned|[poster]|Statherian|Statherian|Constitutes basement beneath the Itiledoo Basin.|c. 1755 Ma|||||
23777|McGregor Volcanics|73234|6|Mentioned|p19|Statherian|Statherian|Associated with Moonabie Formation.|c. 1755 Ma|||||
23777|McGregor Volcanics|73235|6|Mentioned|p53|Statherian|Statherian|Gawler Craton. Olympic and Spencer regions.|1755 Ma|||||
23777|McGregor Volcanics|73493|6|Mentioned|p716 Fig.3|||Gawler Craton.||||||
23777|McGregor Volcanics|73525|6|Mentioned|p19 Fig.13|||Spencer Domain.|||||Felsic volcanics.|
34588|McKinlay Member|13497|5|Briefly described|p115, p115 fig 6.33|Early Cretaceous|Early Cretaceous|Eromanga Basin. Deposited in a lacustrine, shoreface environment. ||Murta Formation||Overlies the Namur Sandstone.|Sandstone.|
34588|McKinlay Member|22839|6|Mentioned|P33|||||||||
34588|McKinlay Member|22883|6|Mentioned|P31|||Parent is the Murta Formation||||||
34588|McKinlay Member|22912|5|Briefly described|33|||Geol province Eromanga Basin||||||
34588|McKinlay Member|23054|6|Mentioned|Fig5p22|Berriasian|Berriasian|||||||
34588|McKinlay Member|23154|6|Mentioned|Map Legend|Early Cretaceous|Early Cretaceous|Geological Province - Eromanga Basin. Parent - Murta Formation.||||||
34588|McKinlay Member|23155|4|Described|p28 & Fig15 on p 28|Early Cretaceous|Early Cretaceous|Unit previously published as a member of the Mooga Formation (Mount, 1982) without definition.  The unit is now defined as a basal member of the Murta Formation, and now includes units N3 and  N4 previously assigned to  Namur Sandstone. Type section p28.||||||31-MAR-09
34588|McKinlay Member|23982|5|Briefly described|p58 Fig.18|||Of Murta Formation. Geological Province: Eromanga Basin.||||||
34588|McKinlay Member|24092|5|Briefly described|p8 Fig.3|||Geological Province: Eromanga Basin.||||||
34588|McKinlay Member|24210|5|Briefly described|p133 Fig. 2|Late Jurassic|Late Jurassic|Of the Murta Formation.  Geological Province: Eromanga Basin.||||||
34588|McKinlay Member|24372|6|Mentioned|p22|||Of the Murta Formation. Geological Province: Cooper Basin.||||||
34588|McKinlay Member|24482|5|Briefly described|p44|Cretaceous|Jurassic|Of the Murta Formation. Geological Province: Eromanga Basin.||||||
34588|McKinlay Member|44133|5|Briefly described|p104 Fig. 9.11, 112|Eraly Cretaceous|Early Cretaceous|Geological Province: Eromanga Basin.||||||
34588|McKinlay Member|60717|5|Briefly described|p40 Fig. 2, p42|Early Cretaceous|Late Jurassic|Of the Murta Formation. Overlies Namur Sandstone. Geological Province: Eromanga Basin.||||||31-JAN-08
34588|McKinlay Member|61615|6|Mentioned|p302 Fig. 2|Early Cretaceous|Late Jurassic|Geological Province: Eromanga Basin.||||||07-FEB-11
34588|McKinlay Member|65489|5|Briefly described|p15, p47, p73, p96, p154-155, p158|Early Cretaceous|Early Cretaceous|Eromanga Basin. Poor-fair reservoir quality. Oil reservoir accounting for 1% of the Basin's production.||Unit in Murta Formation.|||Lacustrine shoreface sandstone.|
34588|McKinlay Member|65925|5|Briefly described|Appendix 2.||||||||Buff, very fine- to medium-grained sandstone interbedded with dark grey carbonaceous and micaceous siltstone.|
34588|McKinlay Member|68068|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Eromanga Basin. Subsurface only. Lake margin and fluvial unit.||Unit at base of Murta Formation.||||
34588|McKinlay Member|69019|5|Briefly described|p85 Fig.21.|Berriasian|Berriasian|Southern Eromanga Basin.||Basal unit in Murta Formation.||Overlies Namur Sandstone.||
34588|McKinlay Member|69023|4|Described|p79, p89 Fig.20, p92-93, p191-192|Berriasian|Berriasian|Of Mount (1982); an undefined unit in the Mooga Formation. Named after Delhi Petroleum exploration well McKinlay 1. Defined as basal Member of Murta Formation by Gravestock et al. (1995). Eromanga Basin. c.12-28m thick. High gamma ray log response. Stratigraphic wells intersection data.||Unit in Murta Formation.||Overlies Namur and Algebuckina Sandstones.|Buff, very fine-grained sandstone, flat to ripple cross-bedded, intensely bioturbated; interbedded with dark grey, laminated to bioturbated, carbonaceous and micaceous siltstone; contains carbonised plant rootlets.|
34588|McKinlay Member|69457|6|Mentioned|p41:3|Early Cretaceous|Early Cretaceous|SW Eromanga Basin. The diagram gives no indication as to which of three units this Member belongs: Algebuckina and Namur Sandstones or Murta Formation.||||||12-JUL-16
34588|McKinlay Member|69673|6|Mentioned|p154, p155 fig 127|Cretaceous|Cretaceous|||||Overlies Namur Sandstone, overlain by Murta Formation||
34588|McKinlay Member|69797|5|Briefly described|p17 Fig.2|Early Cretaceous|Early Cretaceous|Geol. Prov: Eromanga Basin. Presented in figure as McKinlay Mbr.||||||
34588|McKinlay Member|69946|2|Defined|p17-18, p57, p86, p93|Early Cretaceous|Early Cretaceous|Named by Mount (1982), for silty sandstone transitional between Namur Sandstone and Murta Member of the [then] Mooga Formation. Defined by Gravestock et al. (1995) as the basal Member of the Murta Formation. Their type section is the interval 1420.26 - 1436.22m in Strzelecki 4. High gamma ray log response due to elevated U content. Typically <30m thick; often absent in the Cooper region. Eromanga Basin.||Basal unit in Murta Formation.||Intertongues with Murta Formation and the underlying Namur Sandstone.|Micaceous, buff, fine- to medium-grained sandstone interbedded with dark grey carbonaceous siltstone. Strongly bioturbated intervals are characteristic.|
34588|McKinlay Member|69947|5|Briefly described|p8, p13 Fig.7.2, p29 Fig.7.18|Early Cretaceous|Early Cretaceous|Eromanga Basin.||Murta Formation.||Transitionally overlies Namur, Hooray Sandstones.|Fine sandstone and carbonaceous siltstone.|
34588|McKinlay Member|70823|5|Briefly described|p43-p44|Early Cretaceous|Early Cretaceous|Eromanga Basin. Misspelt as the McKinley Member on p44. Deposited in a lacustrine shoreface environment. ||Murta Formation.||Overlies the Namur Sandstone.||
34588|McKinlay Member|71321|6|Mentioned|p15|||Of Eromanga Basin.||||Overlain by Murta Formation.||24-OCT-19
34588|McKinlay Member|71342|3|Fully described|Ch5 p17-p19, Ch5 p32|Berriasian|Berriasian|Eromanga Basin. Originally defined as the silty sandstone transitional between the Namur Sandstone and the Murta Member by Mount (1982). Gravestock et al (1995) defined the unit as a basal member of the Murta Formation and assigned a type section in Strzelecki 4 where the unit has been cored. This unit is typically <30m thick and is often absent in the Cooper region. Age derived from palynology. This unit is interpreted to have been deposited in a low-energy fluvial floodplain environment (Ambrose t al, 1986), however Gravestock et al (1995) propose a shoreface environment on the margin of 'Lake Murta'. Spore-pollen zone is given in Ch5 p57. Forms a seal over the Namur Sandstone. One of the primary petroleum producing units in the Eromanga Basin. See also Ch5 p57, Ch5 p85, Ch5 p93, Ch7 p8, Ch7 p13, Ch8 p5, Ch8 p10, Ch8 p21, Ch10 tbl 10.1, Ch10 p8, Ch10 p20, Ch11 p4-p5, Ch11  p8, Ch11 p17, Ch12 p2, Ch12 p5, Ch13 p2-p5, Ch13 p7, Ch13 p9-p10, Ch13 p17, Ch13 p21, Ch13 p26, Ch13 p29-p31, Ch13 p34, Ch14 p5.||Murta Formation||Intertongues with and overlies the Namur Sandstone. Intertongues with and is overlain by, the Murta Formation.|Micaceous, buff, fine to medium-grained sandstone interbedded with dark grey carbonaceous siltstone.|
34588|McKinlay Member|72298|5|Briefly described|p801|Cretaceous|Cretaceous|Eromanga Basin (SA,QLD). The Table on p801 does not make it at all clear whether this unit in a Member of the Murta FZ or the Namur Sandstone.||Murta FZ.||||
34588|McKinlay Member|73251|6|Mentioned|p62|Early Cretaceous|Early Cretaceous|Eromanga Basin. Contains[?] oil.||||Underlain by Namur Sandstone.||
28742|Melton Limestone|23719|4|Described|p28|Miocene|Miocene|See also page 27 table 8. Overlain by Gibbon Beds. Underlain by Kanaka Beds. Geological Province: Gawler Craton. Max. thickness 10 m.||||||26-MAR-08
28742|Melton Limestone|23768|5|Briefly described|p28 Fig.5|Middle Miocene|Early Miocene|On the Galwer Platform.  See also p61, p82, p103.||||||30-MAR-05
28742|Melton Limestone|23818|5|Briefly described|p174 Fig.84|Early Miocene|Early Miocene|Geological Province: St. Vincent Basin.||||||
28742|Melton Limestone|29856|6|Mentioned|p37|||||||||
28742|Melton Limestone|30251|6|Mentioned|p4|||||||||
28742|Melton Limestone|30807|6|Mentioned|p101|||Suggested map symbol||||||
28742|Melton Limestone|30917|6|Mentioned|p55|||||||||
28742|Melton Limestone|31845|2|Defined|p3|early Miocene|early Miocene|See also p4, 6-9 and Fig. 2.||||||26-MAR-08
28742|Melton Limestone|31850|6|Mentioned|p38|||Refers Lindsay (1970)||||||
28742|Melton Limestone|31919|6|Mentioned|p39|||Miocene||||||
28742|Melton Limestone|32601|6|Mentioned|p686|||||||||
28742|Melton Limestone|33330|6|Mentioned|p167|||||||||
28742|Melton Limestone|34180|6|Mentioned|p221|||Tertiary||||||
28742|Melton Limestone|34308|6|Mentioned|Fig.84|||Correlation chart||||||
28742|Melton Limestone|34536|6|Mentioned|Map legend|Miocene|Miocene|||||||
28742|Melton Limestone|35097|6|Mentioned|Fig.4|||||||||
28742|Melton Limestone|35678|6|Mentioned|Fig.2|||Geological cross-sections, northern Yorke Peninsula.||||||
28742|Melton Limestone|35689|6|Mentioned|Fig.33|||Stratigraphic correlation, St.Vincent Basin.||||||
28742|Melton Limestone|38602|6|Mentioned|p2|||||||||
28742|Melton Limestone|38699|6|Mentioned|p20|||||||||
28742|Melton Limestone|39110|6|Mentioned|p114|||||||||
28742|Melton Limestone|39349|6|Mentioned|Map legend|Miocene|Miocene|||||||
28742|Melton Limestone|40217|6|Mentioned|Map legend|Miocene|Miocene|||||||
28742|Melton Limestone|40448|6|Mentioned|p41|||||||||
28742|Melton Limestone|40643|5|Briefly described|p149|||||||||
28742|Melton Limestone|41043|6|Mentioned|p87|||||||||
28742|Melton Limestone|41505|6|Mentioned|p2|||||||||
28742|Melton Limestone|42536|5|Briefly described|p6|||Yorke Penninsula||||||
28742|Melton Limestone|42731|5|Briefly described|map legend|Miocene||||||||
28742|Melton Limestone|43053|5|Briefly described|Map Legend|Miocene|Eocene|Marine limestone. Geological Province: St Vincent Basin.||||||25-MAY-05
28742|Melton Limestone|43258|5|Briefly described|Map Legend|Miocene|Eocene|||||||
28742|Melton Limestone|43298|6|Mentioned|Map Legend|Miocene|Eocene|||||||
28742|Melton Limestone|43667|6|Mentioned|Fig.3,p12||Miocene|||||||
28742|Melton Limestone|44133|4|Described|p176, 165 Fig. 10.11|Early Miocene|Early Oligocene|Overlies Kanaka Beds; also overlies Tickera Granite in places; underlies Gibbon Beds. Thickness: 32m. Geological Province: Pirie Basin.||||||26-MAR-08
28742|Melton Limestone|44691|4|Described|map legend||Early Miocene|(I/53-12). Lower Miocene.||||||
28742|Melton Limestone|60953|5|Briefly described|Map Legend|Miocene|Eocene|Geological Province: Saint Vincent Basin.||||||
28742|Melton Limestone|60958|5|Briefly described|Map Legend|Miocene|Eocene|Fossiliferous, limestone and sandstone. Geological Province: Saint Vincent Basin.||||||
28742|Melton Limestone|61108|5|Briefly described|map legend|Miocene|Eocene|Geological Province: St Vincent Basin.||||||31-MAY-05
28742|Melton Limestone|61121|5|Briefly described|Map legend|Miocene|Eocene|Fossiliferous, including foramifera 'Lepidocyclinahowchini', limestone and sandstone. Geological Province: St. Vincent Basin.||||||06-JUN-05
28742|Melton Limestone|61155|5|Briefly described|p4, p17|Middle Miocene|Early Miocene|Thin marine, fossiliferous limestones. In the Spencer Gulf area. Age: 21-13.5Ma. Thickness: 10m. Geological Province: Polda Basin, Eyre Peninsula; north St Vincent Basin.||||||
28742|Melton Limestone|64721|5|Briefly described|p11|Miocene|Miocene|Max. thickness: 17m.  Marine marl and limestone which occurs above deposits of Eocene construction sands.||||||
28742|Melton Limestone|65375|5|Briefly described|p33, pp36-37.|Miocene|Oligocene|Equivalent to middle and upper Port Willunga Formation as well as Point Turton Limestone.|||||Fossiliferous limestone and sandstone.|
28742|Melton Limestone|67462|5|Briefly described|Map legend.|Early Miocene|Oligocene|Pirie Basin.|||||Interbedded with un-named lignite layers.|
28742|Melton Limestone|68715|6|Mentioned|p31 Fig.5, p32 Fig.6|Burdigalian|Aquitanian|Pirie Basin.||||||
28742|Melton Limestone|70334|5|Briefly described|p60|Middle Miocene|Late Oligocene|Of Pirie Basin. Thickness: 7-30m on CULTANA. Transgressive sequence deposited between Late Oligocene and early Middle Miocene in a nearshore to shallow marine environment (Lindsay, 1970, Alley and Lindsay, 1995a).||||Overlain by Gibbon Beds. Underlain by Kanaka Beds.|Limestone, calcarenite and calcrudite containing fossils of bryozoa, foraminifera, echinoids and brachiopods; intervals of light yellow-brown fine- to coarse-grained sand and sandstone and calcareous sandy clay.|
28742|Melton Limestone|70382|6|Mentioned|p28|Miocene|Oligocene|Geological province: Troubridge Basin.||||||
28742|Melton Limestone|73103|5|Briefly described|Map legend.|Miocene|Oligocene||||||Bryozoal limestone, sandy and gritty with Lepidocyclina.|
28742|Melton Limestone|73234|6|Mentioned|p23|||Pirie Basin. Marine. Contemporaneous with Neuroodla Formation.||||||
23785|Memory Cove Charnockite|22489|6|Mentioned|p13|||||||||
23785|Memory Cove Charnockite|22629|6|Mentioned|p157|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
23785|Memory Cove Charnockite|22690|6|Mentioned|P306||Orosirian|||||||
23785|Memory Cove Charnockite|24197|5|Briefly described|p74 Tb. 8.1|Paleoproterozoic|Paleoproterozoic|Of the Donington Supersuite? Age: 1840Ma.||||||07-FEB-11
23785|Memory Cove Charnockite|40448|5|Briefly described|Fig.9|||||||||
23785|Memory Cove Charnockite|41667|5|Briefly described|p26|||||||||
23785|Memory Cove Charnockite|43052|5|Briefly described|Table 4.4|||of Donington Granitoid Suite||||||
23785|Memory Cove Charnockite|50605|5|Briefly described|p(i), 1.3, 3.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Age: 1818 +/- 13Ma (Rb-Sr). Of the Donington Granitoid Suite. Geological Province: Gawler Craton & Curnamona Province.||||||07-NOV-08
23785|Memory Cove Charnockite|61070|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Donington Suite. Medium to coarse-grained felsic hypersthene charnockite and enderbite. Locally porphyritic. Magmatitic banding rare. Age: 1850 +/- 6.5Ma (U-Pb Zircon). Geological Province: Gawler Craton.||||||12-JAN-10
23785|Memory Cove Charnockite|65376|4|Described|pp66-68.|||Type locality is Memory Cove on Jussieu Peninsula.|1850 +/- 5 Ma.|Unit in Donington Suite.||Is intruded by Colbert Granite.|Medium-grained hypersthene granodiorite or enderbite.|
23785|Memory Cove Charnockite|66302|6|Mentioned|p27|Orosirian|Orosirian||1850 +/- 5 Ma (SHRIMP, Fanning et al, 2007)|Donington Suite||||
23785|Memory Cove Charnockite|68131|5|Briefly described|p42|Paleoproterozoic|Paleoproterozoic|Eyre Peninsula.||Donington Suite.||||
23785|Memory Cove Charnockite|73027|6|Mentioned|p19-20|Orosirian|Orosirian|||Donington Suite||||
23785|Memory Cove Charnockite|73525|5|Briefly described|p19 Fig.13|Orosirian|Orosirian|Spencer Domain.|1850+/-5 Ma crystallisation age|Donington Suite|||Intermediate intrusive.|
23785|Memory Cove Charnockite|73634|6|Mentioned|p4, 14|||Cape Catastrophe, Eyre Peninsula. Transected by mylonites in high-strain zones.|||||Hypersthene-bearing granite.|
34771|Mena Mudstone Member|22922|6|Mentioned|33 fig 2|||Of Punkerri Sandstone or Narana Formation? Ungoolya Group.||||||
34771|Mena Mudstone Member|23282|2|Defined|p67||Neoproterozoic|Informally defined as Mena Mudstone by Sukanata (1993), now defined as member of Narana Formation. Age: Precambrian, Neoproterozoic, late Marinoan Epoch. of Officer Basin.||||||
34771|Mena Mudstone Member|24112|5|Briefly described|p254 Fig.2|Neoproterozoic|Neoproterozoic|Of the Ungoolya Group. Geological Province: Officer Basin||||||
34771|Mena Mudstone Member|61732|4|Described|p66, p145 Fig. 51|||See also Meena Mudstone Member. Of Narana Fm (Ungoolya Group). Conformably overlies Munta Mudstone Member (Narana Fm); unconformably overlain by Marla Group sediments. Max. thickess: 241m. Geol.Prov: Officer Basin.||||||07-FEB-11
34771|Mena Mudstone Member|72478|6|Mentioned|p8|Marinoan|Marinoan|Officer Basin.|c. 560 Ma|Narana Formation||Overlies the Munta Limestone Member. Unconformably overlain by the Relief Sandstone.||24-MAR-21
34771|Mena Mudstone Member|73099|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Officer Basin.||Narana Formation.||Overlies Munta Limestone Member. Is overlain by Relief Sandstone or Observatory Hill Formation (Marla Group).|Grey to green-grey, laminated to thin-bedded claystone, siltstone, mudstone and minor limestone; thin interbeds of very fine- to coarse-grained sandstone.|
34335|Mentor Formation|22629|5|Briefly described|p162|Proterozoic|Proterozoic|This unit formerly assigned to the Labryinth Formation||||||
34335|Mentor Formation|23490|5|Briefly described|p22|||Formerly Peela Conglomerate Member of Tarcoola Formation.||||||
34335|Mentor Formation|24472|5|Briefly described|p5 Tb.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Harris Greenstone Domain, Gawler Craton.||||||
34335|Mentor Formation|50225|6|Mentioned|p407|||||||||07-FEB-11
34335|Mentor Formation|60515|5|Briefly described|p117|||Associated with the Lower Gawler Range Volcanics.|||||Volcaniclastic sediments.|
34335|Mentor Formation|60953|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Conglomeratic and tuffaceous mudstone to sandstone, granitic breccia.||||||07-NOV-08
34335|Mentor Formation|61108|5|Briefly described|map legend|Mesoproterozoic|Mesoproterozoic|Conglomeratic and tuffaceous mudstone to sandstone and granitic breccia.||||||
34335|Mentor Formation|64130|5|Briefly described|p1383|||Apparently rift-hosted clastic sequence associated with the Gawler Range Volcanics.||||Associated with the Gawler Range Volcanics||
34335|Mentor Formation|64135|6|Mentioned|p1504. |||Central Gawler Craton. Has similarities with the interlayered sedimentary rocks of the Gawler Range Volcanics at Prominent Hill.||||||
34335|Mentor Formation|65385|6|Mentioned|pS128 Fig. 2|||Gawler Craton. Sediments equivalent to the Gawler Range Volcanics.||||||08-MAR-12
34335|Mentor Formation|65390|6|Mentioned|p22 Fig. 3|Mesoproterozoic|Paleoproterozoic|Age of about 1620 - 1565 Ma inferred in Figure 3.||||||26-FEB-15
34335|Mentor Formation|66302|5|Briefly described|p32, p45, p76 Fig.20|||||||Overlies the Labyrinth Formation.|Chloritic and sericitic mudstone, altered and tuffaceous breccia and tuffaceous rhyolite.|
34335|Mentor Formation|72090|6|Mentioned|p12|||Gawler Craton.||Gawler Range Volcanics, Lower||||
34335|Mentor Formation|72459|6|Mentioned|p51|Palaeoproterozoic|Palaeoproterozoic|||||||
34530|Meramangye Formation|22746|4|Described|Fig.3 p515, p519|Neoproterozoic III|Neoproterozoic III|||||||
34530|Meramangye Formation|22922|5|Briefly described|34|||Parent Lake Maurice Group.||||||30-SEP-08
34530|Meramangye Formation|23282|2|Defined|p57||Neoproterozoic|Age: Precambrian, Neoproterozoic, early Marinoan Epoch. was Meramangye beds of Stainton 1988, and Giles Mudstone of Sukanta 1993 and formalised by Zang 1995. of Lake Maurice Group, Officer Basin.||||||
34530|Meramangye Formation|23286|6|Mentioned|p89|||||||||
34530|Meramangye Formation|23524|5|Briefly described|p221 Fig. 3|Neoproterozoic|Neoproterozoic|||||||
34530|Meramangye Formation|24112|5|Briefly described|p254 Fig.2, p257 Tb.1|Neoproterozoic|Neoproterozoic|Of the Lake Maurice Group. Age: 640-615Ma. Geological Province: Officer Basin||||||
34530|Meramangye Formation|44109|5|Briefly described|p22 Fig. 19|Neoproterozoic|Neoproterozoic|Geological Province: central Officer Basin.||||||
34530|Meramangye Formation|61732|5|Briefly described|p13 Tb. 3, p58 Fig. 22|Cryogenian|Cryogenian|Of Lake Maurice Group. Overlain by Murnaroo Formation. Geological Province: Officer Basin. See also p134, p145 Fig. 51.||||||07-FEB-11
34530|Meramangye Formation|63397|2|Defined|27|Neoproterozoic III|Neoproterozoic III|Of the Maurice Group. Type section in text. Red-brown and minor green-grey silty mudstone interbeds with thin siltstone or fine-grained sandstone. Thickness: 243m. Conformably overlies Tarlina Sandstone and conformably underlies Murnaroo Formation.||||||18-JUL-07
34530|Meramangye Formation|64724|5|Briefly described|p49 Fig. 7|Ediacaran|Ediacaran|Deposited in the Officer Basin during the Centralian 3 event (~600-544 Ma)||||||
34530|Meramangye Formation|64794|6|Mentioned|p238 fig 2, p244 |Ediacaran|Ediacaran|||Lake Maurice Group||Overlies Tarlina Formation (conformably). Overlain by Murnaroo Formation (conformably),|Marine mudrock.|
34530|Meramangye Formation|64797|6|Mentioned|p153 Fig.2|Ediacaran|Ediacaran|Officer Basin. Lithology/rank not shown on diagram.||||||
34530|Meramangye Formation|65892|6|Mentioned|p35.|Late Neoproterozoic|Late Neoproterozoic|Eastern Officer Basin. Is equivalent to Brachina Formation in Adelaide Geosyncline.||||||
34530|Meramangye Formation|66569|5|Briefly described|p861 fig.2,|Ediacaran|Ediacaran|Unconformably underlies Murnaroo Sandstone; unconformably overlies Tarlina Sandstone.||||||
34530|Meramangye Formation|67620|6|Mentioned|p22|||Officer Basin. Contains abundant organic laminae (microbial mats).||||||
34530|Meramangye Formation|68269|6|Mentioned|p674|Ediacaran|Ediacaran|||||Unconformably underlain by Tarlina Sandstone. Unconformably overlain by Murnaroo Sandstone.|Sandstone/siltstone dominated.|
34530|Meramangye Formation|69648|4|Described|p17-19, map legend|Neoproterozoic|Neoproterozoic|Transgressive to highstand. Age: Marinoan. Probable equivalents of this unit have been interpreted from drillhole logs. Lithologies originally interpreted as Cambrian Observatory Hill Formation in SADME Ooldea 3 have been tentatively correlated with Meramangye Formation on OOLDEA map sheet. Max thickness, if stratigraphic correlation is correct: 85.7m (in drillhole SADME Ooldea 3).||Lake Maurice Group||Underlying Tarlina Sandstone grades upwards (conformable); overlying Murnaroo Formation continuously shallows-upwards (conformable).|Transgressive to highstand siltstone and silty mudstone.|17-FEB-15
34530|Meramangye Formation|72478|6|Mentioned|p8|Ediacaran|Cryogenian|Officer Basin. Age shown as Marinoan.|c. 650 Ma-615 Ma|||Shown as unconformably overlying Tarlina Sandstone. Conformably overlain by Murnaroo Formation.||24-MAR-21
34530|Meramangye Formation|72601|6|Mentioned|p5, p10|||Officer Basin.||||||
34530|Meramangye Formation|73099|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Officer Basin.||Lake Maurice Group.||Overlies Tarlina Sandstone. Is overlain by Murnaroo Formation.|Reddish grey to brown, laminated, micaceous siltstone and claystone with minor fine-grained sandstone.|
34530|Meramangye Formation|73392|6|Mentioned|p3||||||||Sampled from core of Giles 1 well.|
80743|Merdayerrah Shoshonite|72242|5|Briefly described|p30-31,34|Stenian|Stenian|Geological province: Coompana Province, Western Gawler Craton. Associated with Maralinga Event (including Musgrave Orogeny). Intersected in the CDP004 drillhole. Contains relative juvenile EHF1074Ma values and suggests little to no assimilation of pre-1900 Ma crust; appears to be product of mantle input and crustal assimilation similar to Bunburra and Koomalboogurra suites (Dutch 2018). Provides a link between previously enriched lithospheric mantle and the crustal magmatism. Magmatism with shoshonitic affinities has been found to be associated with Cu/Cu-Au deposits globally (e.g. Bingham Canyon Cu-Au-Mo; Groves and Santosh 2015).|c. 1174 Ma|||||
80743|Merdayerrah Shoshonite|72344|5|Briefly described|p7, p9, p76|Stenian|Stenian|Coompana Province. Intersected in drillholes CDP004. Petrography, SHRIMP analyses and geochemistry are discussed for a sample.|1174 +/- 9 Ma (SHRIMP magmatic age)|Koonalda Suite|||Foliated dark green quartz-syenite.|
80743|Merdayerrah Shoshonite|72947|2|Defined|p7, p9, p12-14, p21|Stenian|Stenian|Coompana Province, eastern. Named after Merdayerrah Sandpatch. No known surface exposures. Not assigned to a suite. Type locality: CDP004 (drillhole 299058, interval ~672.5-677.6 m); which is the only drillhole the unit is recognised in. Represents high-grade metamorphism, anatexis, deformation and magmatism. The rock is called a shoshonite, based on geochemical characteristics. Relatively juvenile eHf1174-1140 Ma values suggest little or no assimilation of any pre-1900 Ma crust; appear to be the product of mantle input and assimilation of crust (Dutch, 2018). Derived from the same modified lithospheric mantle source that produced the Warbla Suite. Solid-state foliation that is defined by aligned biotite flakes in the equigranular groundmass. Rare irregular centimetre-wide feldspar xenocrysts. Forms sheets with a maximum thickness of 5 m. Sharp intrusive margins within the Bunburra Suite including quenched margins.|1174 +/- 9 Ma SHRIMP U-Pb|Moodini Supersuite||May correlate to Bottle Corner Shoshonite. Intrudes Bunburra Suite.|Brown to dark green, fine- to medium-grained, granoblastic-textured metamorphosed quartz syenite, which contain feldspar, hornblende and biotite.|
80743|Merdayerrah Shoshonite|73084|6|Mentioned|p129|Stenian|Stenian|Geochemically very similar to the Bottle Corner Shoshonite, although slightly more evolved. Age from Jagodzinski and Bodorkos (2018).|1174 +/- 9 Ma|||Intrudes Bunburra Suite.|Includes quartz metasyenite.|
80743|Merdayerrah Shoshonite|73224|5|Briefly described|p42-43|Stenian|Stenian|Product of mantle input and the assimilation of crust similar to the Bunburra and Koomalboogurra suites.|1174 +/- 9 Ma||||Mafic-intermediate composition.|
80743|Merdayerrah Shoshonite|73225|5|Briefly described|p4, 14, 17|||Eastern Coompana Province. Drill-hole; not exposed. Represents deep melting of subduction-enriched subcontinental lithospheric mantle during extension.|1174 +/- 9 Ma (Jagodzinski et al., 2019).||||Occurs as sheets and lenses in migmatites. Biotite flakes define solid-state foliation.|
26734|Merinjina Tillite|22510|5|Briefly described|table 1, p36,38|||"Wooltana" area. Age: Sturtian||||||
26734|Merinjina Tillite|23913|4|Described|p108, p110 Fig. 2|Adelaidean|Adelaidean|Geological Province: Central Flinders Zone.  Of the Umberatana Group.  Overlying Unit: Tapley Hill Formation.||||||05-JUL-13
26734|Merinjina Tillite|24476|4|Described|p547 Fig. 4|Adelaidean|Adelaidean|Overlain by the Tapley Hill Formation.  Geological Province: Adelaide fold belt.||||||
26734|Merinjina Tillite|24546|5|Briefly described|p2 - 3 Fig.2|Neoproterozoic|Neoproterozoic|Of Umberatana Group. Geological Province: Adelaide Fold Belt.||||||16-JAN-08
26734|Merinjina Tillite|30178|6|Mentioned|p19|||||||||
26734|Merinjina Tillite|36137|4|Described|p11|||Palaeomagnetism discussed.||||||
26734|Merinjina Tillite|36198|6|Mentioned|p324|||||||||
26734|Merinjina Tillite|36733|6|Mentioned|Table 5|||||||||
26734|Merinjina Tillite|36837|6|Mentioned|p52|||||||||
26734|Merinjina Tillite|37461|6|Mentioned|Table 5.I|||||||||
26734|Merinjina Tillite|37932|3|Fully described|p541|||||||||
26734|Merinjina Tillite|39344|6|Mentioned|Map legend|Precambrian|Precambrian|Sturtian||||||
26734|Merinjina Tillite|40254|6|Mentioned|p284|||||||||
26734|Merinjina Tillite|41258|6|Mentioned|p18|||||||||
26734|Merinjina Tillite|41400|6|Mentioned|p27|||||||||
26734|Merinjina Tillite|41405|3|Fully described|p148|||||||||
26734|Merinjina Tillite|42222|6|Mentioned|p16|||||||||
26734|Merinjina Tillite|42779|5|Briefly described|Table 1 P287|||||||||
26734|Merinjina Tillite|43052|5|Briefly described|p183,Table 6.1|||||||||
26734|Merinjina Tillite|62428|5|Briefly described|p351 Tb. 6||Neoproterozoic III|Palaeomagnetic data.||||||10-FEB-09
26734|Merinjina Tillite|64846|5|Briefly described|p197 Fig.2, p198 Fig.3, p208 Fig.10 |Cryogenian|Cryogenian|Sturtian glaciation. Age from a tuffaceous horizon.|658 Ma (U-Pb zircon: Fanning and Link, 2006).|Of the Yudnamutana Subgroup.||||
26734|Merinjina Tillite|65493|5|Briefly described|p910, Fig 1,2,6,13|Cryogenian|Cryogenian|Of Yudnamutana Subgroup. Conformably and disconformably overlain by Tapley Hill Formation. Sturtian aged glacial diamictites, in northern Adelaide Geosyncline.||||||
26734|Merinjina Tillite|65925|5|Briefly described|p124 Fig.3.|||||Unit in Umberatana Group.|||Massive diamictite.|
26734|Merinjina Tillite|67180|6|Mentioned|p601 Fig.1, p602 Fig.2, p611 Fig.10|Cryogenian|Cryogenian|Sturtian age.||Unit in Yudnamutana Subgroup||Conformably underlies the Tapley Hill Formation (Tindelpina Shale Member).||
26734|Merinjina Tillite|67979|5|Briefly described|p529, p531 Fig.2|Sturtian|Sturtian|In Northern Flinders Ranges||Yudnamutana Subgroup||abruptly overlain by Tindelpina Shale Member (of Tapley Hill Formation)|diamictites|
26734|Merinjina Tillite|68271|5|Briefly described|p697|||Contains a tuff in the upper section with U-Pb zircon SHRIMP age of c. 658 Ma, representing a later phase of Sturtian glacials in northern Flinders Ranges (Fanning and Link, 2006).||||||
26734|Merinjina Tillite|70021|6|Mentioned|p97|Neoproterozoic|Neoproterozoic|Northern Flinders Ranges, Adelaide Geosyncline.||||||
26734|Merinjina Tillite|70082|6|Mentioned|p2|Cryogenian|Cryogenian|Flinders Ranges. Contains marine till.||||||
26734|Merinjina Tillite|70383|6|Mentioned|p46|Cryogenian|Cryogenian|Exposed in the Stubbs Waterhole area, ~9 km SSE of Mount Gee. Looks similar to the Sprigg Diamictite Member.||||||
26734|Merinjina Tillite|70384|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Adelaide Geosyncline. Age shown more specifically as Sturtian [Cryogenian].||Yudnamutana Subgroup.|||Diamictite with abundant quartzite and rhyolite clasts east of Paralana Fault Zone.|21-JAN-19
26734|Merinjina Tillite|72613|6|Mentioned|p2 fig 1|Neoproterozoic|Neoproterozoic|Northern Flinders Ranges. See also the Merinjina Diamictite. || Of Yudnamutana Subgroup, Umberatana Group.||||
34792|Mernmerna Formation|22766|5|Briefly described|Fig.2 p561, p567|Early Cambrian|Early Cambrian|||||||
34792|Mernmerna Formation|23562|5|Briefly described|p295 Fig 2|Cambrian|Neoproterozoic III|||||||
34792|Mernmerna Formation|23981|5|Briefly described|p8-9 Fig. 4, p10 Fig. 5, p51, p55|Early Cambrian|Early Cambrian|Nodular, fine-gr. med.grey limestones interbedded with v. calcareous mudstones; lithology varies from area to area.Transitional up into Orapinna Shale. Overlies lower Wilkawillina Lst in Yalkalpo Syncline; Intertongues with Wirrapowie Lst. GeolProv: Arrow||||||
34792|Mernmerna Formation|24465|5|Briefly described|p345 Fig.2|Early Cambrian|Early Cambrian|Of the Hawker Group.  Geological Province: Arrowie Basin.||||||19-JAN-05
34792|Mernmerna Formation|44133|5|Briefly described|p4 Fig. 7.2, 23|Early Cambrian|Early Cambrian|Geological Province: Arrowie Basin. Overlies lower Wilkawillina Limestone.||||||
34792|Mernmerna Formation|60418|4|Described|p133|Botoman-Atdabanian|Botoman-Atdabanian|Of the Hawker Group. Overlies Second Plain Creel Member. Disconformably overlain by Bunkers Sandstone. Thickness at type section: 800m. Max. thickness: 2500m. Contains type speciman of mollusc Tannuella elinorae. Geological Province: Arrowie Basin||||||
34792|Mernmerna Formation|60889|4|Described|p245 Fig.2, p248-9, p251-2, p254|Early Cambrian|Early Cambrian|Platformal carbonates. Thickness varies greatly: 100-500 m in many Arrowie Basin sections, up to 800 m in the Bunkers Graben and more than 2500 m in the Nepabunna Trough. Arrowie Basin.|526 +/- 4.0 Ma; 526.6 +/- 1.6 Ma.|Hawker Group||Overlies lower Wilkawillina Limestone. Is overlain by middle Wilkawillina Limestone. Intertongues with Midwerta Shale and Nepabunna Siltstone. Relationship with upper Andamooka Limestone is unclear.|Deep water. Slope facies carbonates and siltstones. Nodular limestone. Nodular and flaggy.|21-SEP-17
34792|Mernmerna Formation|60959|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of the Hawker Group. Dark grey, fine grained, nodular to mottled, well bedded limestone to shaly limestone.||||||
34792|Mernmerna Formation|60990|5|Briefly described|p83 Fig.2, p85 |Botoman|Atdbanian|Flinders Ranges. Faunal links with Antarctica.||Hawker Group.||||
34792|Mernmerna Formation|62783|6|Mentioned|p2 Fig.1|||||||||
34792|Mernmerna Formation|62784|4|Described|p8-10, pp12-15, p18, p26, p33|Early Cambrian|Early Cambrian|Arrowie Basin. Type section at Wilkawillina Gorge. Fossil age constraint.||Of Hawker Group.|Includes Six Mile Bore, Third Plain Creek and Linns Springs Members.|Unconformably overlies Wilkawillina Limestone, disconformably overlain by Bunkers Sandstone.||20-MAR-12
34792|Mernmerna Formation|62790|6|Mentioned|p207|Early Cambrian|Early Cambrian|Contains the phosphatocopid Dabashanella hemicyclica and six bradoriid taxa from the Pararaia bunyerooensis Zone (Botoman).||||||
34792|Mernmerna Formation|63447|5|Briefly described|p961,p962,p963 Fig.2 |Early Cambrian|Early Cambrian|Equivalent to the Parara Limestone [Stansbury Basin]||Hawker Group||Shown as lateral equivalent to Midwerta Shale, Nepabunna Siltstone, Bendieuta Formation, Wilkawillina Limestone, Bunkers Sandstone, Oraparinna Shale, Moorowie Formation, Ajax Limestone.||
34792|Mernmerna Formation|63569|4|Described|pp116-124, p127, p136|Lower Cambrian|Lower Cambrian|Arrowie Basin, Adelaide Geosyncline. Contains rich assemblage of silicified trilobites, often severely abraded due to transport by turbidity currents and debris flows. Eoredlichia fragments resemble South China specimens.||Unit in Hawker Group.|Includes Third Plain Creek, Six Mile Bore and Linns Springs Members.|Overlies Wilkawillina Limestone; contact is a red microstromatolite horizon representing the Flinders Unconformity. Is disconformably overlain by Bunkers Sandstone.|Interbedded black turbiditic wackestone-packstone and laminated lime silt and mud; rare sandstone beds. Grain flow deposits, irregular and nodular bedding  common.|
34792|Mernmerna Formation|65375|5|Briefly described|p33.|Early Cambrian|Early Cambrian|||Unit in Hawker Group.||Overlies Wilkawillina Limestone. Is overlain by Bunkers Sandstone.||
34792|Mernmerna Formation|65686|5|Briefly described|p411, 413, 415, 420, p409 Fig 2-4,5|Early Cambrian|Early Cambrian|Arrowie Basin, 800m thick.||||||
34792|Mernmerna Formation|65892|5|Briefly described|p9 Fig.4, p10, p12, p28-31, p44. |Early Cambrian|Early Cambrian|Arrowie Basin. 800m thick. Slope facies carbonates and siltstones. Contains the mollusc Tannuella elinorae. Bioturbation is common in upper levels. Appears also as Mernamerna Formation on p10.||Unit in Hawker Group.||Intertongues with Midwerta Shale and Nepabunna Siltstone. Is overlain by Oraparinna Shale.|Mottled and dark silty limestone; well-bedded fine-grained sandstone; quite chert-rich in top 50m.|
34792|Mernmerna Formation|65925|5|Briefly described|p14 Fig.2.2, Appendix 2.|Early Cambrian|Early Cambrian||||||Limestone; bioherm complexes. Slope, platform bioherm complexes, distal slope environments; turbidites; nodular wackestone; black laminated lime mud.|
34792|Mernmerna Formation|66518|6|Mentioned|p19 Fig.4.|Cambrian|Cambrian|Arrowie Basin. ||Unit in Hawker Group.||Unconformably overlies Wilkawillina Limestone. Is overlain by Moorowie Formation.||
34792|Mernmerna Formation|67870|6|Mentioned|p10|||Source of bituminous hydrocarbons recovered from this unit.||||||
34792|Mernmerna Formation|67907|6|Mentioned|p260|||Flinders Ranges. Pararaia bunyerooensis trilobite Zone (Topper et al., 2009).||||||
34792|Mernmerna Formation|68030|5|Briefly described|p239|Cambrian|Cambrian|Flinders Ranges. Contains Ediacaran stromatolites and archaeocyathids.||Unit of Hawker Group.||Overlain unconformably by Billy Creek Formation. Underlain unconformably by, and laterally grades into Wilkawillina Limestone.||
34792|Mernmerna Formation|68735|4|Described|p233 Fig.2, p234, p235 Fig.3|Early Cambrian|Early Cambrian|Arrowie Basin. Shows considerable thickness variations (100-500 m thick in many areas; up to 800 m thick in Bunkers Graben; over 2500 m thick in the Nepabunna Trough). Intraformational slumping is present towards the top of the formation.||Of the Hawker Group.||Underlain by the Wilkawillina Limestone. Interfingers with the Midwerta Shale and Nepabunna Siltstone. Overlain and interfingered by the Oraparinna Shale.|Comprises dark slope carbonates and calcareous siltstones.|
34792|Mernmerna Formation|68993|6|Mentioned|p544 Fig.1|Early Cambrian|Early Cambrian|Arrowie Basin.||Of the Hawker Group.||||
34792|Mernmerna Formation|69570|6|Mentioned|p421 fig 1, p433, p435|Cambrian|Cambrian|Arrowie Syncline, Flinder Ranges.||||||
34792|Mernmerna Formation|70833|4|Described|p176,179,181-2,186-7,190,194-5,198-203|Series 2|Series 2|Of Arrowie Basin. MOG (S of Moro Gorge, Arrowie Syncline); MMT (Bunkers Range, central Flinders Ranges); WILK (Bunkers Graben); 10MS-W (Ten Mile South, SE Bunkers Graben). Contains nodular limestone beds, deposited in low energy, outer shelf, ramp and sope settings, with input from allochthonous carbonates containing slumps or slide structures, indicating active shelf collapse and slope processes. Includes the D. odyssei zone. Also appears as Upper Mernmerna Formation on p201.||Unit of Hawker Group.|Includes Six Mile Bore, Linns Springs and Third Plain Creek members. Time-equivalent to Parara Limestone and upper part of Heatherdale Shale.|||08-AUG-19
34792|Mernmerna Formation|70835|5|Briefly described|p334-338, 340, 343, 346, 349, 351|Cambrian|Cambrian|Chace Range, southern Flinders Ranges. Contains silicified macro-scale univalves of Helcionellid and other species (described in great detail). Photographs. See also p354-355.||Hawker Group.|Six Mile Bore, Linns Springs, Third Plain Creek, Members.|Overlies Wirrapowie Limestone conformably and Wilkawillina Limestone unconformably. Is overlain by Oraparinna Shale or Bunkers Sandstone.|Lower part has fine micritic, dark limestones.|
34792|Mernmerna Formation|71102|4|Described|p242-252,254,256,258|Series 2|Series 2|Of Arrowie Basin. Interpreted as a carbonate ramp-slope facies. Contains large allochthonous blocks derived from older collapsed platform deposits (mainly Wilkawillina) recorded in the Bunkers Range at Bonkey Bore Syncline (see p252 for references). Intersected sections: ER9 (Elder Range, Southern Flinders Ranges), DBS (Donkey Bore Syncline), 10MS (10 Mile South, Bunkers Graben), RC (Rainwater Creek, S Arrowie Syncline), NB (North Boundary Creek, Chambers Gorge, E Flinders Ranges), PIN (Pinyatta Creek, Chambers Gorge). Fossil assemblage described. See also on p263-265,266-267,269-273.|||Includes Third Plain Creek, Linns Springs and Six Mile Bore members, and Midwerta Shale(?) and Nepabunna Siltstone.|Overlain by Moorowie Formation or Bunkers Sandstone or Oraparinna Shale. Underlain by, and interfingers with Wilkawillina or Wirrapowie limestones.|Bedded, micritic ribbon limestone. Minor oolitic and sandy beds. Dark coloured, flaggy, calcareous mudstones and wackestones, common spiculitic (mainly hexactinellid) horizons.|05-SEP-19
34792|Mernmerna Formation|72429|2|Defined|p949, p952, p958, p960-970, p974, p976|Early Cambrian|Early Cambrian|Mount Chambers Gorge, eastern Flinders Ranges; Arrowie Basin. Tuffs record contemporaneous volcanism with rapid changes in sedimentary facies. Subdivided into a lower, middle and upper undifferentiated units. Internal variation is discussed. Trilobites. Previously rocks were described as the Parara Limestone of Daily, 1956. The equivalent 'Parara' unit was redefined as Mernmerna Formation. This unit is widely preserved, mapped and well studied for rich fossil faunas. The lower part of the Mernmerna Formation correlates with the C1.2 transgressive cycle of Gravestock and Hibburt (1991). Extensive outcrops were mapped and measured in the Moorowie area, supported by exceptional exposures of fresh rock along many ravines. Five divisions were recognised, units 2, 4 and 6 are of similar offshore marine character. Unit 2 is inferred to have been deposited in a dysoxic marine basin, set on a low-angle carbonate ramp below storm wave base, regularly punctuated by periodic currents of variable strength. Suspended clay or carbonate whitings may have restricted light-penetration into the seas. Includes three species of tommotiids, four species of brachiopods and three species of bradoriids. Units 3 and 5 are interpreted as localised interbeds of trough margin or evaporite diapir-island association, inserted into the more-regional marine basin deposits. Includes a number of unnamed upper beds that are described further. Deposited in a deep-marine dysoxic ramp environment as a result of a largely single catastrophic collapse of a thick carbonate buildup below wave base.||Hawker Group|Includes the Bendieuta Member.|Conformably overlies the Wilkawillina Limestone. Underlies the Moorowie Formation.|Well-bedded, grey laminated limestones with thin interbeds of black carbonaceous and calcareous shales; syndepositional slump-induced intraformational folds and breccias, collapse talus and graded sediment gravity flows.|
34792|Mernmerna Formation|72449|5|Briefly described|p1, p2 Map Legend|Cambrian|Cambrian|||||Overlies Wilkawillina Limestone and underlies Oraparinna Shale, Bunkers Sandstone.|Bedded, dark grey, fine grained, nodular to mottled limestone and shaly limestone.|
34792|Mernmerna Formation|73251|6|Mentioned|p36|Cambrian|Cambrian|Arrowie Basin, Moorowie and Yalkalpo Sub-basins. Thermally late to post-mature. May include oil-prone organic facies.||Hawker Group||Unconformably underlain by Wilkawillina Limestone. Overlain by Moorowie Formation.||
34792|Mernmerna Formation|74367|5|Briefly described|p19|Cambrian|Cambrian|Arrowie Basin. Ages including 514.56+/-0.13 Ma are detrital zircon TIMS ages from three tuff layers (Betts et al., 2018).|515.38+/-0.13 Ma, 514.46+/-0.13 Ma TIMS zircon|||Stratigraphically equivalent to Heatherdale Shale.||
38101|Michell Nob Granite|24301|4|Described|p13, p6 Tb. 1|Mesoproterozoic|Mesoproterozoic|Overlain by Nulchara Charnockite.  Geological Province: Musgrave Block||||||
38101|Michell Nob Granite|60679|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Granite. Geological Province: Musgrave Block.||||||
38101|Michell Nob Granite|61154|5|Briefly described|p14, p28|Mesoproterozoic|Mesoproterozoic|Felsic intrusion in N.T. near Mulga Park Station. Coarse-grained, porphyritic and contains phenocrysts of K-feldspar as well as plagioclase, quartz, biotite, garnet and amphibole.  Age: 1068+/-6Ma (SHRIMP U-Pb zircon: Camacho 1997). See also p13, p44 App.||||||
38101|Michell Nob Granite|63866|5|Briefly described|p206|Stenian|Stenian|Musgrave Province.|1068 +/- 6 Ma (Camacho, 1997, SHRIMP U-Pb)|||||
38101|Michell Nob Granite|67128|4|Described|p3, p12, p27-28, p30|||Mulga Park area, Musgrave Ranges. Also appears as Michael Nob Granite on p12 and p30. Strongly deformed during the Petermann Orogeny.|1068 +/- 13 Ma (Camacho, 1997).|||Is crosscut by Nulchara Charnockite.|Mesocratic, K-feldspar porphyritic to rapakivi-textured, hornblende-orthopyroxene-biotite-garnet bearing granite. Mylonitic: up to 3cm subrounded microcline and perthite phenocrysts wrapped by granoblastic fabric.|
38101|Michell Nob Granite|69436|5|Briefly described|p21:11-12|Mesoproterozoic|Mesoproterozoic|Young et al. (2002). Occurs in a small area, on the SA border, near Mulga Park station. Musgrave Province. Emplaced during the Giles Event (1085-1040 Ma). SHRIMP U-Pb zircon age.|1068 +/- 6 Ma (Camacho, 1997).|Warakurna Supersuite.|||Coarse-grained K-feldspar-porphyritic granite, with plagioclase, quartz, biotite, garnet and amphibole. Has a strong, anastomosing mylonitic fabric. Biotite and hornblende define a mineral elongation parallel to the stretching lineation.|12-JUL-16
38101|Michell Nob Granite|70018|5|Briefly described|p235|||Amadeus Basin. Comagmatic with Nulchara Charnockite based on presence of Nulchara Charnockite xenoliths in the MNG and vice versa. Average 207Pb/206Pb age (Jaffey et al., 1971) is 1074.3+\-0.9 Ma.||||Overlain by Nulchara Charnockite.|Porphyritic with large (up to 3 cm) sub-rounded, simply twinned crystals of K-feldspar wrapped by a finer-grained mylonitic fabric.|
38101|Michell Nob Granite|71592|5|Briefly described|Appendix A.|||Musgrave Province.|1068+/-6 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granite.|
28125|Midwerta Shale|22766|6|Mentioned|p567|||||||||
28125|Midwerta Shale|23981|5|Briefly described|p8-9 Fig. 4, p10 Fig. 5|Early Cambrian|Early Cambrian|Geological Province: Arrowie Basin.||||||
28125|Midwerta Shale|24176|1|Redefined|p38 Appendix|Early Cambrian|Early Cambrian|See also p17 and p23 Tb.1.  Grey-green shale and calcareous shale, minor nodular limestone.  Intertongues with Parara Limestone.  Max. thickness: 132m.  Geological Province: Mount Painter Province.||||||17-JUL-07
28125|Midwerta Shale|30176|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
28125|Midwerta Shale|30807|6|Mentioned|p102|||Suggested map symbol||||||
28125|Midwerta Shale|31730|6|Mentioned|p100|||Geochem. Stream sediment sampling.||||||
28125|Midwerta Shale|35255|6|Mentioned|Fig.8|||||||||
28125|Midwerta Shale|36198|6|Mentioned|Fig.I.2|||||||||
28125|Midwerta Shale|42011|6|Mentioned|Fig.3 P458|||||||||
28125|Midwerta Shale|42225|6|Mentioned|Fig.4 P224|||||||||
28125|Midwerta Shale|42272|6|Mentioned|p414|||||||||
28125|Midwerta Shale|42440|6|Mentioned|Fig.2 P602|||||||||
28125|Midwerta Shale|42458|5|Briefly described|Fig.2 P699|||||||||
28125|Midwerta Shale|44133|5|Briefly described|p4 Fig. 7.2, 23|Early Cambrian|Early Cambrian|Geological Province: Arrowie Basin. Intertounges with Mernmerna Formation.||||||
28125|Midwerta Shale|60418|5|Briefly described|p135|Early Cambrian|Early Cambrian|Of the Hawker Group. Geological Province: Arrowie Basin of Adelaide Geosyncline.||||||18-MAY-05
28125|Midwerta Shale|60889|4|Described|p247 Fig.4, p248, p251|Early Cambrian|Early Cambrian|North-Central Trough, Arrowie Basin.||Hawker Group||Intertongues with Midwerta Shale and Nepabunna Siltstone.|Siltstone.|21-SEP-17
28125|Midwerta Shale|60959|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of the Hawker Group. Grey-green shale and calcareous shale, minor nodular limestone.||||||
28125|Midwerta Shale|63447|6|Mentioned|p963 Fig.2 |Early Cambrian|Early Cambrian|||||Shown as lateral equivalent to upper Wilkawillina Limestone in part, Bendieuta Formation, Nepabunna Siltstone, Mernmerna Formation (Parara Limestone) in part.||
28125|Midwerta Shale|63569|6|Mentioned|p117 Fig.1|Early Cambrian|Early Cambrian|Arrowie Basin.||||||
28125|Midwerta Shale|65892|5|Briefly described|p9 Fig.4, p10. |Early Cambrian|Early Cambrian|Arrowie Basin. In Angepena-Nepabunna area, interfingers with nodular limestone of the Mernmerna Formation.||Unit in Hawker Group.||||
28125|Midwerta Shale|65925|5|Briefly described|p14 Fig.2.2, Appendix 2.|Early Cambrian|Early Cambrian||||||Green-grey to black shale, argillaceous pyritic and manganiferous.|
28125|Midwerta Shale|68735|6|Mentioned|p234|||||Hawker Group.||Interfingers with the Mernmerna Formation.|Fine-grained clastic unit.|10-APR-17
28125|Midwerta Shale|68993|6|Mentioned|p544 Fig.1|Early Cambrian|Early Cambrian|Arrowie Basin.||Of the Hawker Group.||||
28125|Midwerta Shale|69570|6|Mentioned|p421 fig 1|Cambrian|Cambrian|Arrowie Syncline, Flinder Ranges.||||||
28125|Midwerta Shale|71102|5|Briefly described|p242,247,249|||Of Arrowie Basin. Previous mapping in the Angepena, Nepabunna and Arrowie synclines in the northern Flinders Ranges showed the Midwerta Shale to be a unit of Mernmerna Formation (e.g. Coats etal., 1973 ;Gravestock, 1995; Zang etal. ,2004), but could also be a unit of Wirrapowie Limestone based on lithology. Intersected section: BHG (Bullock Head Gap, SW Arrowie Syncline)|||||Grey to buff unfossiliferous silty shale.|
83177|Mikkira Granite|73122|5|Briefly described|p23, 25, 29-32, 42|||Syn- to post-Kimban Orogeny. After the first mention, it appears as Mikkira granite in the text, casting doubt as to the author's intention to regard the name as formal. Mikkira Granite is used in several figures.||Moody Suite.|||Hornblende-bearing granite; contains xenoliths of orthogneiss.|12-APR-22
39565|Milendella Member|24465|4|Described|p347|Early Cambrian|Early Cambrian|Of the Blowhole Creek Member (Carrickalinga Head Formation) - occuring as thin units of marble-calc-silicate within the Blowhole Creek Member.   Replaces Milendella Limestone Member.||||||19-JAN-05
39565|Milendella Member|63848|6|Mentioned|p534 Fig.4.|||||Unit in Carrickalinga Head Formation.||||
25679|Miltalie Gneiss|22629|5|Briefly described|p149, fig2p147, fig4|Orosirian|Orosirian|Age: 2003+/-13 Ma.||||||23-JUL-13
25679|Miltalie Gneiss|22690|6|Mentioned|P305||Orosirian|Age of unit is 2014+/-28 Ma||||||
25679|Miltalie Gneiss|23285|5|Briefly described|Fig 1 p 332|||||||||
25679|Miltalie Gneiss|23481|5|Briefly described|p19 Fig 1|||Geological Province: Gawler Craton.||||||
25679|Miltalie Gneiss|23719|4|Described|p12|Statherian|Statherian|Age: 1697+/-65 Ma (Rb-Sr), see also p14 table 1. Overlain by Hutchinson Group. Underlain by Sleaford Complex. Geological Province: Gawler Craton.||||||29-APR-09
25679|Miltalie Gneiss|23791|5|Briefly described|p4, p20|Paleoproterozoic|Paleoproterozoic|Geological Province: Gawler Craton.||||||07-NOV-08
25679|Miltalie Gneiss|23803|5|Briefly described|p28|Paleoproterozoic|Paleoproterozoic|Geological Province: Gawler Craton.||||||07-NOV-08
25679|Miltalie Gneiss|23805|5|Briefly described|p4 Fig. 1|Paleoproterozoic|Paleoproterozoic|Geological Province: Gawler Craton.||||||07-NOV-08
25679|Miltalie Gneiss|24197|5|Briefly described|p17, p74 Tb. 8.1|Paleoproterozoic|Paleoproterozoic|Age: 2015Ma. Geological province: Gawler Craton.||||||07-FEB-11
25679|Miltalie Gneiss|24505|5|Briefly described|p5 Fig. 1|||Geological Province: Gawler Craton.||||||
25679|Miltalie Gneiss|24508|6|Mentioned|p30|||Geological Province: Gawler Craton.||||||19-SEP-05
25679|Miltalie Gneiss|39345|6|Mentioned|Map legend|Paleoproterozoic|Archean|Archaean - Early Proterozoic||||||07-NOV-08
25679|Miltalie Gneiss|39349|6|Mentioned|Map legend|Paleoproterozoic|Archean|Archaean to Early Proterozoic||||||07-NOV-08
25679|Miltalie Gneiss|39353|6|Mentioned|Map legend|Paleoproterozoic|Archean|Archaean to Early Proterozoic||||||07-NOV-08
25679|Miltalie Gneiss|39802|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
25679|Miltalie Gneiss|40227|6|Mentioned|p44|||||||||
25679|Miltalie Gneiss|40448|5|Briefly described|p27|||Age: 2003+/-13 Ma.||||||23-JUL-13
25679|Miltalie Gneiss|40644|5|Briefly described|p120, p127 Fig. 6|Paleoproterozoic|Archean|Of Parker (1983). Included in the Sleaford Complex . Age: 1697+/-65Ma; age range of ca.2100Ma (Plug Range) to 2315Ma (Minbrie Springs) also presented. Geological province: Gawler Craton.||||||07-NOV-08
25679|Miltalie Gneiss|41667|4|Described|p11|||||||||
25679|Miltalie Gneiss|41972|4|Described|p371|||||||||
25679|Miltalie Gneiss|42934|5|Briefly described|p524|||||||||
25679|Miltalie Gneiss|43052|4|Described|p52|||Minimum age of 2014+/-28 Ma||||||
25679|Miltalie Gneiss|43053|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Gneiss and amphibolite.||||||07-NOV-08
25679|Miltalie Gneiss|43258|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
25679|Miltalie Gneiss|43298|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
25679|Miltalie Gneiss|50219|5|Briefly described|p259, p275|Orosirian|Orosirian|Age: ca. 2000Ma.  Geological Province: Gawler Craton.||||||07-FEB-11
25679|Miltalie Gneiss|50333|5|Briefly described|p12|Paleoproterozoic|Paleoproterozoic|Age: ca. 2000Ma.||||||07-NOV-08
25679|Miltalie Gneiss|50605|5|Briefly described|p(i), 2.1|Paleoproterozoic|Paleoproterozoic|Age: 2014-2015+/- 28Ma (U-Pb). Geological Province: Gawler Craton & Curnamona Province. Of the Miltalie Suite. Intrudes Sleaford Complex.||||||07-NOV-08
25679|Miltalie Gneiss|60515|6|Mentioned|p116 Fig.1 |||||||||
25679|Miltalie Gneiss|60534|5|Briefly described|p572 Fig.1, 573 Fig.2|Paleoproterozoic|Paleoproterozoic|Age: ~2000 Ma. Geological Province: Gawler Craton.||||||07-NOV-08
25679|Miltalie Gneiss|60953|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Age: 2003-1999Ma. Granitic orthogneiss.||||||07-NOV-08
25679|Miltalie Gneiss|60954|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Gawler Craton.||||||07-NOV-08
25679|Miltalie Gneiss|61070|5|Briefly described|Map Legend|Paleoproterozoic|Archean|Well-foliated, medium to coarse-grained, pink-grey migmatitic granite gneiss, granite to granodiorite. Unconformably overlain by Hutchison Group. Emplacement age: 2003 +/- 18Ma (U-Pb Zircon). Geological Province: Gawler Craton.||||||23-JUL-13
25679|Miltalie Gneiss|61108|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|Granitic orthogneiss. Age: 2003-1999 Ma.||||||07-NOV-08
25679|Miltalie Gneiss|61522|5|Briefly described|p5 Fig.1|||Geological Province: Gawler Craton.||||||
25679|Miltalie Gneiss|63223|5|Briefly described|p16, p17 Fig. 1, p19|Paleoproterozoic|Archean|Age: ~2000Ma. Geological Province: Gawler Craton.||||||07-NOV-08
25679|Miltalie Gneiss|63224|6|Mentioned|p10|||Geological Province: Gawler Craton.||||||07-FEB-08
25679|Miltalie Gneiss|63866|4|Described|p5, p19|Orosirian|Orosirian|Cleve Domain. Forms the crystalline basement to the Cleve Domain.|c. 2000 Ma (U-Pb zircon)|||Unconformably overlain by the Hutchison Group.|Migmatitic quartzo-feldspathic gneiss.|
25679|Miltalie Gneiss|64130|5|Briefly described|p1378 Fig.1, p1379, p1380 Fig.2, p1384  |Paleoproterozoic|Paleoproterozoic|Crops out discontinuously over 250 km.|ca. 2000 Ma (Fanning et al., 1988)|||Unconformably underlies the Hutchison Group.|Granodioritic.|
25679|Miltalie Gneiss|64722|5|Briefly described|Fig. 2 p3-6, p13, 24|Orosirian|Orosirian|Thought to be emplaced during extensional tectonism.|~2000 Ma.|||Unconformably overlain by Hutchison Group.|Orthogneiss.|11-APR-12
25679|Miltalie Gneiss|64739|6|Mentioned|p264 Fig.1. |Paleoproterozoic|Paleoproterozoic|Gawler Craton.||||||
25679|Miltalie Gneiss|65221|5|Briefly described|p26|Palaeoproterozoic|Palaeoproterozoic|Felsic precursor of this unit intruded the Sleaford Complex||||||
25679|Miltalie Gneiss|65375|5|Briefly described|p13.|Paleoproterozoic|Paleoproterozoic|Basement rock in Eyre Peninsula, Gawler Craton.|1996-1991 Ma.|||Is unconformably overlain by Hutchison Group.||
25679|Miltalie Gneiss|65376|5|Briefly described|p8 Fig.1.1, pp45-53. |Paleoproterozoic|Paleoproterozoic||2001 +/- 8 Ma.||||Granitic gneiss.|
25679|Miltalie Gneiss|65390|5|Briefly described|p19, p20, p23 Fig.3|Orosirian|Orosirian|Cleve Domain, Gawler Craton. Has a zircon crystallisation age of c.2000 Ma (Fanning, 1997). Unconformably underlies Hutchison Group.||||||
25679|Miltalie Gneiss|65483|6|Mentioned|p17 Fig. 1|Palaeoproterozoic|Palaeoproterozoic|||||||
25679|Miltalie Gneiss|65485|6|Mentioned|p42, Fig 1|Paleoproterozoic|Paleoproterozoic|Contains 2000 Ma metamorphic zircons.||||||19-MAR-12
25679|Miltalie Gneiss|65772|5|Briefly described|p229 Fig.2, p234 Fig.8|Paleoproterozoic|Paleoproterozoic|~2000 Ma. Ortho- and paragneiss.||||||
25679|Miltalie Gneiss|65915|5|Briefly described|p2|Orosirian|Orosirian|Overlies Sleaford Complex. Overlain by Hutchison Group. ~2000 Ma (Fanning et al., 2007).||||||
25679|Miltalie Gneiss|65922|5|Briefly described|p12, p13 Fig.4, p29 Fig. 6|Orosirian|Orosirian|Cowell-Cleve area, Gawler Craton. Age of ~2000-1960 Ma given. ||||||
25679|Miltalie Gneiss|66302|5|Briefly described|p4 Fig.3, p18, p25, p26, p33, p56, p62|Orosirian|Orosirian|Cleve Domain, Southern Gawler Craton. Protoliths of this unit intruded at approximately 2020-2000 Ma and may have been emplaced in an extensional tectonic regime. Age derived from SHRIMP U-Pb dating by Fanning et al. (2007).|2002 +/- 15 to 1999 +/- 9 Ma|||Equivalent to the Glengarra Granite.|Migmatitic and quartzofeldspathic gneiss.|
25679|Miltalie Gneiss|66882|5|Briefly described|p101, p102 Fig.2, p105, p114 Figs.11,12|Orosirian|Orosirian|See also p116-117, p120. Part of basement complex for Hutchison Group in the Lincoln-Cleve uplands region. Possible source rocks for Cleve Group.|2002+/-15 Ma and 1999+/-13 Ma|||Unconformably underlies Warrow Quartzite.||
25679|Miltalie Gneiss|67058|5|Briefly described|p476.||||Precursor intruded c.2000 Ma.|||Is overlain by Hutchison Group.|Granodioritic gneiss.|
25679|Miltalie Gneiss|67536|5|Briefly described|Map Legend|Orosirian|Orosirian|Gawler Craton.|2003 +/- 18 Ma - 1997 +/- 11 Ma||||Migmatised granodioritic gneiss.|
25679|Miltalie Gneiss|67581|6|Mentioned|p44 Fig.8|||||||||
25679|Miltalie Gneiss|67721|5|Briefly described|p34, p36 Fig.6|Orosirian|Orosirian||c. 2000 Ma|||||
25679|Miltalie Gneiss|68131|5|Briefly described|p2 Fig.1|Paleoproterozoic|Paleoproterozoic||||||Granitic gneiss.|
25679|Miltalie Gneiss|68208|6|Mentioned|p32 Fig.3|Archean|Archean|[Archean age shown in legend to Fig 3 may be erroneous. Probably Paleoproterozoic]||||||
25679|Miltalie Gneiss|69048|6|Mentioned|p1, p3|Paleoproterozoic|Paleoproterozoic|Southern Eyre Peninsula. Age of granite precursors.|c.2000 Ma.|||||
25679|Miltalie Gneiss|69554|6|Mentioned|p130, 139|Paleoproterozoic|Paleoproterozoic|Fanning et al. (2007). Eastern Gawler Craton.|c.2020-2000 Ma.|||||
25679|Miltalie Gneiss|69649|6|Mentioned|p6 Fig.4|||||||||
25679|Miltalie Gneiss|70027|6|Mentioned|p56,58|Orosirian|Orosirian|Geological province: Gawler Craton. Intruded by magmatic rocks during 1730-1690 Ma Kimban Orogeny.|ca. 2000 Ma|||||
25679|Miltalie Gneiss|70286|6|Mentioned|p884|Paleoproterozoic|Paleoproterozoic|Eastern Gawler Craton.|c.2000 Ma.|||||
25679|Miltalie Gneiss|70382|6|Mentioned|p32|Paleoproterozoic|Paleoproterozoic|Geological province: eastern Gawler Craton.  Possible source for some of Quartoo Sand Member inherited zircon.|~2020-2000 Ma||||Gneiss|
25679|Miltalie Gneiss|70405|6|Mentioned|p12 figure 4|Paleoproterozoic|Paleoproterozoic||2000 Ma|||||
25679|Miltalie Gneiss|70721|6|Mentioned|p73|||||||||
25679|Miltalie Gneiss|71043|6|Mentioned|p107|||Southern Gawler Craton.|c.2000 Ma.|||||
25679|Miltalie Gneiss|71129|6|Mentioned|p14,p17-18,203|Rhyacian|Rhyacian|Geological Province: Cleve-Coulta Domain, Gawler Craton.|c.2000 Ma|||||13-NOV-19
25679|Miltalie Gneiss|71235|6|Mentioned|p13||||c. 2000 Ma (Fanning et al, 2007)|||||
25679|Miltalie Gneiss|71236|5|Briefly described|p2|Palaeoproterozoic|Palaeoproterozoic|||||||
25679|Miltalie Gneiss|71317|5|Briefly described|p15-p16|Palaeoproterozoic|Palaeoproterozoic|Cleve-Coulta Domains, Gawler Craton.|2000 Ma|||||
25679|Miltalie Gneiss|71318|5|Briefly described|p3,47|Paleoproterozoic|Paleoproterozoic|Geological province: Gawler Craton. Sample GSSA 2017971 (medium-grained granite gneiss) yielded an interpreted (weighted mean 207Pb/206Pb) magmatic crystallisation age of 2010+\-13 Ma.||||||
25679|Miltalie Gneiss|71534|5|Briefly described|p296.300|Orosirian|Orosirian|Geological province: Gawler Craton. Localised magmatism associated with onset of sediment deposition in the Gawler Craton (Fanning et al., 2007). Hf isotope analysis indicates mixing of mantle and crustal material.|c. 2020 Ma|||||
25679|Miltalie Gneiss|71559|6|Mentioned|p15 Fig 1|Paleoproterozoic|Paleoproterozoic|Geological province: Gawler Craton.||||||
25679|Miltalie Gneiss|71859|5|Briefly described|p3-p6, p18, p35|Paleoproterozoic|Paleoproterozoic|Cleve and Coulta domains, southern Gawler Craton. Appears as the Miltallie Gneiss on p3 and Miltalile Gneiss on p4.|c. 2000 Ma (ign. Precursor)|||||
25679|Miltalie Gneiss|71862|6|Mentioned|p3-p4|||||||||
25679|Miltalie Gneiss|72090|6|Mentioned|p10, p11|Orosirian|Orosirian|Cleve-Coulta Domain, Gawler Craton.|2000 Ma|||||
25679|Miltalie Gneiss|72242|6|Mentioned|p27|Orosirian|Siderian|Geological province: Coompana Province, Western Gawler Craton. Bomidal magmatism associated with Miltalie Event.||||||
25679|Miltalie Gneiss|72459|6|Mentioned|p51|Paleoproterozoic|Paleoproterozoic|Coulta/Cleve domains.|2003 +/- 13 Ma|||||
25679|Miltalie Gneiss|72462|6|Mentioned|p3|Paleoproterozoic|Paleoproterozoic|Gawler Craton.||||||
25679|Miltalie Gneiss|72527|6|Mentioned|p192.|Paleoproterozoic|Paleoproterozoic|Of Gawler Craton. Zircons of ca 2000 Ma characterise this unit (e.g. Fraser and Neumann, 2010).|c. 2000 Ma|||||
25679|Miltalie Gneiss|73026|5|Briefly described|p4 fig1.2, p5-6, p9|Paleoproterozoic|Paleoproterozoic|Central/western Eyre Peninsula. Felsic protoliths to this unit were emplaced at c. 2000 Ma. Occurs structurally below the Hutchison Group.|c. 2000-1608 Ma||||Gneiss, migmatitic.|
25679|Miltalie Gneiss|73027|5|Briefly described|p4-p6, p9|Palaeoproterozoic|Palaeoproterozoic|Central/western Eyre Peninsula.|c. 2000 Ma||||Gneiss, migmatitic.|
25679|Miltalie Gneiss|73030|6|Mentioned|p2149|Orosirian|Orosirian|Gawler Craton.||||||
25679|Miltalie Gneiss|73061|6|Mentioned|p1076 Fig.5, p1077|||Gawler Craton.||||||
25679|Miltalie Gneiss|73103|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Is also shown in the Solid Geology Interpretation map, below the main Whyalla 250k map.|||||Gneiss, migmatitic grey granitic, coarse-grained equigranular foliated, quartz, perthitic, microcline, plagioclase, biotite.|
25679|Miltalie Gneiss|73122|6|Mentioned|p17, p18 Fig.1||||2000 Ma.|||||
25679|Miltalie Gneiss|73130|6|Mentioned|[poster]|Orosirian|Orosirian|Constitutes basement beneath the Itiledoo Basin.|c. 2000 Ma|||||
25679|Miltalie Gneiss|73234|6|Mentioned|p18|Orosirian|Orosirian|Age from Fanning, Reid and Teale (2007)[?].|c. 2000 Ma|||||
25679|Miltalie Gneiss|73493|5|Briefly described|p716 Fig.3|||Gawler Craton.|||||Granitic, deformed.|
25679|Miltalie Gneiss|73634|6|Mentioned|p2 Fig.1|Archean|Archean|Eyre Peninsula, Gawler Craton. Appears in Fig.1 as Sleaford Complex +/- Miltalie Gneisses.||||||
30615|Miltalie Suite|50605|5|Briefly described|p1.3, Table 1.1|Paleoproterozoic|Paleoproterozoic|Age: 2014Ma. Geological Province: Gawler Craton & Curnamona Province.||||||07-NOV-08
34768|Mimili Formation|22922|6|Mentioned|34|Late Devonian|Late Devonian|Officer Basin.||||||
34768|Mimili Formation|23282|2|Defined|p83-83, 49,||Frasnian|Age: Late Devonian, Frasnian 375-360Ma. May correlate with Pertnjara Group and possibly Mereenie Sandstone of the Amadeus Basin. Type section: surface to 1018 m in Munyarai 1 well. 3 informal sub-units: Basal fine to medium-grained micaceous and occasionally calcareous clean arkosic sandstone. Middle is fossil-bearing and composed of interbedded greenish grey micaceous, calcareous mudstone with minor siltstone and fine to medium-grained sandstone. The uppermost unit generally ferruginised, muddy brown arkosic sandstone.||||||13-DEC-21
34768|Mimili Formation|23858|5|Briefly described|p917|||Underlying unit Blue Hills Sandstone. Geological Province: Officer Basin. Max. thickness ~1000 m.||||||
34768|Mimili Formation|24112|5|Briefly described|p254 Fig.2|Late Devonian|Late Devonian|Geological Province: Officer Basin||||||
34768|Mimili Formation|60953|5|Briefly described|Map Legend|Devonian|Devonian|Non-marine arkosic sandstone, calcareous mudstone and siltstone.||||||
34768|Mimili Formation|61108|5|Briefly described|map legend|Devonian|Devonian|Non-marine arkosic sandstone, calcareous mudstone and siltstone. Age: ?Devonian.||||||
34768|Mimili Formation|64970|6|Mentioned|p719 Fig. 2|Carboniferous|Devonian|Geological Province: Officer Basin.||||||27-MAY-09
34768|Mimili Formation|65376|6|Mentioned|p9 Fig.1.2, p247 Fig.6.57.|Devonian|Devonian|||||||
34768|Mimili Formation|68131|5|Briefly described|p2 Fig.1|Devonian|Devonian|Non-marine sediments.||||||
34768|Mimili Formation|71146|5|Briefly described|p6|Famennian|Emsian|Officer Basin.||||Unconformably overlies the Blue Hill Sandstone (Munda Group).|Sandstone.|
34768|Mimili Formation|72476|6|Mentioned|p36 Fig.9|||Officer Basin. Time-temperature thermal history diagram.||||||
34768|Mimili Formation|72478|6|Mentioned|p8|Late Devonian|Late Devonian|Officer Basin.|c. 375-355 Ma|||Unconformably overlies the Blue Hills Sandstone. Unconformably underlies the Boorthanna Formation.||
23793|Minbrie Gneiss|22629|6|Mentioned|p157|Proterozoic|Proterozoic|||||||
23793|Minbrie Gneiss|22849|5|Briefly described|20|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
23793|Minbrie Gneiss|23719|4|Described|p19|Paleoproterozoic|Paleoproterozoic|Age: ~1850-1800 Ma. See also page 19 table 5. Part of the Lincoln Complex. Geological Province: Gawler Craton.||||||07-NOV-08
23793|Minbrie Gneiss|23731|6|Mentioned|p26|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
23793|Minbrie Gneiss|24197|5|Briefly described|p74 Tb. 8.1|Paleoproterozoic|Paleoproterozoic|Age: >1800Ma.||||||07-FEB-11
23793|Minbrie Gneiss|24505|6|Mentioned|p9 Tb. 1|||Geological Province: Gawler Craton.||||||
23793|Minbrie Gneiss|24526|6|Mentioned|p98|||Probably correlates with the Donnington and Colbert Granitoid Suites.||||||14-JUN-05
23793|Minbrie Gneiss|24567|5|Briefly described|p160 Tb. 2|Paleoproterozoic|Paleoproterozoic|Age: ca1800Ma. Geological Province: East Gawler Craton.||||||07-NOV-08
23793|Minbrie Gneiss|39345|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
23793|Minbrie Gneiss|39349|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
23793|Minbrie Gneiss|39353|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
23793|Minbrie Gneiss|39802|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
23793|Minbrie Gneiss|40448|5|Briefly described|p34|||||||||
23793|Minbrie Gneiss|40644|6|Mentioned|p126|||Part of the Lincoln Complex. See also Fig.8||||||13-AUG-08
23793|Minbrie Gneiss|41667|5|Briefly described|p11|||||||||
23793|Minbrie Gneiss|43052|5|Briefly described|Table 4.4|||Of Lincoln Complex.||||||23-JUN-09
23793|Minbrie Gneiss|50605|5|Briefly described|p(i), 4.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Gawler Craton and Curnamona Province. Age: >1800Ma (Rb-Sr). Of the Minbrie Suite.||||||07-NOV-08
23793|Minbrie Gneiss|61307|5|Briefly described|p36 Fig. 17, p37|Paleoproterozoic|Paleoproterozoic|Deformed hornblende-bearing granodiorites and augen gneisses; contains xenoliths of Warrow Quartzite. Age: 1851+/-332Ma. Geological Province: Gawler Craton.||||||07-NOV-08
23793|Minbrie Gneiss|62893|6|Mentioned|p13|||Of Parker (1983).||||||
23793|Minbrie Gneiss|65376|4|Described|pp37-40, p80. |||A number of variably deformed granite gneisses at Refuge Rocks. Revised geochronology takes this unit out of Donington Suite; further, the quartzite rafts cannot be of Warrow Quartzite, as thought previously.|2413 +/- 7 Ma.|Unit in Sleaford Complex.|||Composed of two phases: a medium-grained granodiorite gneiss; a strongly foliated megacrystic augen gneiss. Both contain rafts of quartzite.|
23793|Minbrie Gneiss|65390|5|Briefly described|p17-18, p23 Fig.3|Orosirian||Cowell-Cleve region, northern Eyre Peninsula; considered a Donington Granitoid Suite equivalent. Consists of granite gneiss, granodiorite gneiss and augen gneiss; multiply deformed and with enclaves of Hutchison Group metasediments. The granite gneiss has a Rb-Sr age of >1800 Ma (Webb et al. 1986).||||||
23793|Minbrie Gneiss|66302|6|Mentioned|p14|Siderian|Neoarchean||2520 Ma - 2455 Ma |Sleaford Complex||||
23793|Minbrie Gneiss|68208|6|Mentioned|p32 Fig.3|Paleoproterozoic|Paleoproterozoic|||||||
23793|Minbrie Gneiss|69048|6|Mentioned|p57|||Central Eyre Peninsula. Contains metamorphic zircon aged 1762 +/- 43 Ma (Fraser and Neumann, 2010); this predates the usual Kimban Orogeny time interval.||||||
23793|Minbrie Gneiss|70721|6|Mentioned|p63-p64|Archean|Archean||c. 2550-2440 Ma|||||
23793|Minbrie Gneiss|71129|6|Mentioned|p204|||Geological province: Gawler Craton. Contains metamorphic growth zircons dated at 1762+\-43 Ma (Fraser and Neumann, 2010); affected by same c. 1775 Ma deformation event as the Tip Top Granite and Wertigo Granite.||||||
23793|Minbrie Gneiss|71235|6|Mentioned|p9|Palaeoproterozoic|Palaeoproterozoic|||||||
23793|Minbrie Gneiss|71322|6|Mentioned|p103|Paleoproterozoic|Paleoproterozoic|Northern Eyre Peninsula.||||||
23793|Minbrie Gneiss|71859|3|Fully described|p1-p2, p6-p7, p14-p15|Paleoproterozoic|Neoarchean|Southern Gawler Craton. First used by Parker & Flint, 1983 and described in detail in the accompanying explanatory notes of Parker and Fanning, 1998. The name is derived either from the Minbrie Range, Minbrie Homestead, Minbrie Spring or Minbrie Hill. No type locality has been defined but reference localities have been suggested by Parker and Fanning (1998) at Elbow Hill, Minbrie Springs, Salt Creek and Refuge Rocks; descriptions at these localities can be found in Parker et al., 1988; Parker, 1993; Fraser and Neumann (2010) and Jagodzinski and McAvaney (2016). Previously assigned to the palaeoproterozoic Lincoln Complex before geochronology recognised it as part of the Sleaford Complex. Magnesian, calc-alkalic to alkalic and peraluminous in composition. Likely derived from remelting of a source region similar to the Coolanie Gneiss. Occurs in the Cleve Hills as a northeast- to north-trending curvilinear belt, 95km long and 3km wide at its southern end widening to 25km in the North. Inferred structural contact with the Coolanie Gneiss and Hutchison Group. Igneous protoliths interpreted primarily as monzonite to granitic in composition. Geochemistry analysis and results are discussed. See also p17-p26, p28-p29, p35-p36.|c. 2520-2420 Ma U-Pb zircon|Sleaford Complex||Intruded by the Middle Camp Granite and the Peter Pan Supersuite. Interleaved (structurally) with the Hutchison Group.|Heterogenous unit consisting of granitic gneiss, quartz-feldspar-biotite migmatitic gneiss and minor paragneiss and sills of amphibolite.|11-APR-23
23793|Minbrie Gneiss|71862|5|Briefly described|p2, p8, p11-p12, p53, p60|Neoarchean|Neoarchean|Originally a part of the now obsolete Lincoln Complex.|c. 2520-2420 Ma|||Intruded by the Middle Camp Granite and the Moola Suite.||
23793|Minbrie Gneiss|72462|6|Mentioned|p10|||Formed during the Kimban Orogeny from a Sleaford Complex precursor.|||||Medium- to very coarse-grained quartz-feldspar-biotite migmatitic gneiss.|
23793|Minbrie Gneiss|73026|6|Mentioned|p19|Statherian|Statherian||1762 +/- 43 Ma|||||
23793|Minbrie Gneiss|73027|6|Mentioned|p46||||1762 +/- 43 Ma (SHRIMP U-Pb)|||||
23793|Minbrie Gneiss|73103|5|Briefly described|Map legend.|Paleoproterozoic|Archean|Metamorphosed at 1738 - 1733 Ma (U-Pb).|2521 - 2411 Ma (crystallisation).||||Granite gneiss; augen gneiss; migmatitic gneiss, layered; pegmatite; amphibolite. Upper amphibolite to granulite facies.|
23793|Minbrie Gneiss|73110|5|Briefly described|Map legend.|Paleoproterozoic|Archean|Metamorphosed 1738 - 1733 Ma (U-Pb).|2521 - 2411 Ma (crystallisation).|Sleaford Complex.|||Granite gneiss; augen gneiss; migmatitic gneiss, layered; pegmatite; amphibolite. Upper amphibolite to granulite facies.|
41690|Minbrie Suite|50605|5|Briefly described|p1.3, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Gawler Craton and Curnamona Province. Age: >1800Ma.||||||07-NOV-08
26741|Minburra Quartzite|22889|6|Mentioned|p39|Adelaidean|Adelaidean|The Stratigraphic position of this unit is uncertain,  ? member of the Saddleworth Formation or it may correlate with the Leasingham Quartzite Member, Further work is required to resolve this.||||||
26741|Minburra Quartzite|29780|6|Mentioned|p28|||||||||
26741|Minburra Quartzite|30801|6|Mentioned|p5|||Torrensian. Table P5-6||||||
26741|Minburra Quartzite|30807|6|Mentioned|p103|||Suggested map symbol||||||
26741|Minburra Quartzite|32724|6|Mentioned|Fig.1|||Correlation. Torrensian||||||
26741|Minburra Quartzite|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Torrensian||||||
26741|Minburra Quartzite|41404|5|Briefly described|p114|||||||||
26741|Minburra Quartzite|42222|6|Mentioned|p14|||||||||
26741|Minburra Quartzite|43052|5|Briefly described|p181|||||||||
26741|Minburra Quartzite|44659|5|Briefly described|map legend|||Torrensian, lithology.||||||
75894|Mindamereeka Trondhjemite|67540|3|Fully described|p25, p27 Tb.1, p28 Tb.2, p38 Fig.2|Calymmian|Calymmian|Type locality: Crockers Well Original Mine, extending 1.6 km SE towards Ethiudna Hill. Curnamona Province: Olary Domain. Definition reference: this article and Fricke and Hore (2011). High-U and high-U/Th radiometric signature.|1580 +/- 21 Ma|Of the Crocker Well Suite.|||White, coarse-grained and massive leucocratic phlogopite trondhjemites grading into sodic alaskites characterised by opalescent blue quartz.|08-FEB-16
75894|Mindamereeka Trondhjemite|69562|5|Briefly described|p669, p671 Tb.5|||S Lake Frome region. Up to 110 ppm U. Has undergone intensive sodic metasomatism.|1580 +/- 21 Ma (Ludwig and Cooper, 1984).|Unit in Crocker Well Suite.|||White, coarse-grained and massive, leucocratic phlogopite trondhjemites grading into alaskites, characterised by opalescent blue quartz.|
75894|Mindamereeka Trondhjemite|69650|2|Defined|p4-5 Tbs.1,2; p12, p21-24, p26-27, p29|Calymmian|Calymmian|New name, after Mindamereeka Hill, 43 km NNW of Manna Hill. Type locality: At Crockers Original Mine (GDA 94 386846 mE, 6457573 mN) extends 1.6km SW towards Ethiudna Hill. Extreme enrichment in U and Th. The alaskites occur as dykes, veins and irregular bodies within the trondhjemites. Generally surrounded by Mount Victoria Granite. Geochemistry outlined.|1580 +/- 21 Ma U-Pb zircon; Ludwig & Cooper, 1984|Unit in Crocker Well Suite.||Intrudes Mount Victoria Granite.|White, coarse-grained and massive leucocratic phlogopite trondhjemites grading into sodic alaskites characterised by opalescent blue quartz; minor alaskite pegmatite.|25-NOV-22
75894|Mindamereeka Trondhjemite|70658|5|Briefly described|p33-36|Mesoproterozoic|Mesoproterozoic|Restricted to the Crocker Well region, Olary Domain, Curnamona Province. Geochemistry briefly described.|1580 +/- 21 Ma.|Crocker Well Suite.|||White, coarse-grained and massive leucocratic phlogopite trondhjemites grading into sodic alaskites characterised by opalescent blue quartz.|
38067|Minke Supersequence|24336|5|Briefly described|p99 Fig.3|||Correlated to the Echidna Formation.||||||
38067|Minke Supersequence|61544|6|Mentioned|p367 Fig.3. |Berriasian|Tithonian|Ceduna Sub-basin. Syn-rift mechanical extension.||||Overlies Sea Lion Supersequence. Is overlain by Southern Right Supersequence.||
38067|Minke Supersequence|66578|6|Mentioned|p1007 Fig.3.|Early Cretaceous|Late Jurassic|Ceduna Sub-Basin, Bight Basin.||||Overlies Sea Lion Supersequence.||
38067|Minke Supersequence|69297|5|Briefly described|p14 fig 2.4, p23, p25 fig 2.9|Tithonian|Tithonian|Eyre, Ceduna and Duntroon Sub-basins. Shale facies within this sequence have the best potential to be seal rocks in the Eyre Sub-basin. Good faulting seal capacity for hydrocarbons. Contains potential source rocks within lacustrine shales and coaly deposits. See also p26 fig 2.11, p27, p28, p37, p42, p45 fig 2.17, p58, p60, p61. ||||Overlies the Sea Lion Supersequence. Overlain by the Southern Right Supersequence.|Sandstone, siltstone and claystone.|
38067|Minke Supersequence|70067|5|Briefly described|Ceduna: Fig.2. Regional: Fig.2|Berriasian|Tithonian|Bight Basin. Includes the Echidna Formation (except the topmost part); the lithologies are unknown, not having been penetrated by wells.||||Overlies Sea Lion Supersequence. Is overlain by Southern Right Supersequence.||
28756|Minlaton Formation|22643|5|Briefly described|p186, fig3,6|Early Cambrian|Early Cambrian|||||||
28756|Minlaton Formation|22766|5|Briefly described|Fig.2 p561, p563|Early Cambrian|Early Cambrian|||||||
28756|Minlaton Formation|23981|5|Briefly described|p8-9 Fig. 4, p10 Fig. 5|Toyonian|Early Cambrian|Fine to med.gr. sandstone,calc. siltstone, sandy lst; wavy bedded sandy lst with streaks of shale. Overlies Parara Lst passing transitionally into Koolywurtie Lst Mbr below; conformably/disconformably underlies Ramsay Fm. Geol.P: Stansbury Basin.||||||04-FEB-08
28756|Minlaton Formation|24360|5|Briefly described|p53|Cambrian|Cambrian|Geological Province: Yorke Peninsula, Gawler Craton||||||
28756|Minlaton Formation|24465|5|Briefly described|p343, p345 Fig. 2|Early Cambrian|Early Cambrian|Geological Province: Stansbury Basin.||||||19-JAN-05
28756|Minlaton Formation|35255|6|Mentioned|Fig.8|||||||||
28756|Minlaton Formation|40856|6|Mentioned|Fig.23.6|||||||||
28756|Minlaton Formation|41526|6|Mentioned|p61|||||||||
28756|Minlaton Formation|42222|6|Mentioned|p21|||||||||
28756|Minlaton Formation|42225|4|Described|p222|||||||||
28756|Minlaton Formation|42269|5|Briefly described|p336|||See also Fig.1||||||
28756|Minlaton Formation|42488|5|Briefly described|Fig.2 P187|||||||||
28756|Minlaton Formation|43053|5|Briefly described|Map Legend|Cambrian|Cambrian|Shallow marine to terrestrial redbeds, peritidal to marine limestone.||||||25-MAY-05
28756|Minlaton Formation|43258|5|Briefly described|Map Legend||Cambrian|||||||
28756|Minlaton Formation|43298|6|Mentioned|Map Legend||Cambrian|||||||
28756|Minlaton Formation|43759|6|Mentioned|p451|||||||||
28756|Minlaton Formation|44133|5|Briefly described|p4 Fig. 7.2, 12, 15, 17|Early Cambrian|Early Cambrian|Geological Province: Stansbury Basin. Overlies: Koolywurtie Member. Overlain by: Ramsay Limestone (transitionally).||||||
28756|Minlaton Formation|60958|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Red-brown and minor grey siltstone, sandstone, silty carbonate and basal conglomerate. Gypsum layers at top. Geological Province: Stansbury Basin.||||||14-APR-05
28756|Minlaton Formation|61121|5|Briefly described|Map legend|Early Cambrian|Early Cambrian|Red-brown and minor grey grey siltstone, sandstone, silty carbonate and basal conglomerate.  Gypsum layers at the top.  Age is Toyonian. Geological Province: Stansbury Basin.||||||06-JUN-05
28756|Minlaton Formation|64282|5|Briefly described|Map legend|Early Cambrian|Early Cambrian|Geological Province: Stansbury Basin. Red-brown and minor grey siltstone, sandstone, silty carbonate and basal conglomerate. Gypsum layers at the top.||||||24-JUL-08
28756|Minlaton Formation|65375|4|Described|pp26-30.|Early Cambrian|Early Cambrian|Red-beds. No outcrops, but widely intersected in drillholes.||||Unconformably overlies Winulta Formation and Parara Limestone. Is overlain by Ramsay Limestone.|Red-brown and minor grey siltstone, sandstone, silty carbonate and conglomerate; several gypsum layers in the upper part.|
28756|Minlaton Formation|65686|6|Mentioned|p413|Early Cambrian|Early Cambrian|Stansbury Basin||||||
28756|Minlaton Formation|65892|5|Briefly described|p9 Fig.4. |Early Cambrian|Early Cambrian|Yorke Peninsula.||||Overlies Parara Limestone. Is overlain by Ramsay Limestone.||
28756|Minlaton Formation|66761|6|Mentioned|p254|Cambrian|Cambrian|Yorke Peninsula. Correlated with Kanmantoo Group and Kangaroo Island Group, in part.||||||14-MAR-12
28756|Minlaton Formation|68735|6|Mentioned|p233, p233 Fig.2, p235 Fig.3|Early Cambrian|Early Cambrian|Stansbury Basin. The base of this formation correlates with the bases of both the Kanmantoo Group and the Billy Creek Formation and the Kanmantoo Group.||||||
28756|Minlaton Formation|68993|6|Mentioned|p544 Fig.1|Early Cambrian|Early Cambrian|Yorke Peninsula.||||||
28756|Minlaton Formation|70833|5|Briefly described|p200|Cambrian|Cambrian|Of Western Stansbury Basin.||||Overlain by Ransay Limestone. Underlain unconformably by Parara Limestone.||
28756|Minlaton Formation|70835|6|Mentioned|p354|||Yorke Peninsula. Lower Cambrian. Mentioned in connection with macromollusc fossils.||||||
28756|Minlaton Formation|73107|5|Briefly described|Map legend.|Early Cambrian|Early Cambrian|Stansbury Basin.|||||Red-brown and minor grey siltstone, sandstone, silty carbonate and basal conglomerate. Gypsum layers at the top. Marginal marine, deltaic, fluvial to lacustrine. Acritarchs and shelly fossils. Subsurface only. Toyonian.|
28756|Minlaton Formation|73247|6|Mentioned|p205|Cambrian (Stage 4)|Cambrian (Stage 4)|Yorke Peninsula.||||Unconformably underlain by Parara Limestone. Equivalent to Smith Bay Shale and Stokes Bay Sandstone.||
40401|Mirage Granite|24422|6|Mentioned|p102 Fig. 13a|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Woods Inlier, Gawler Craton.||||||07-NOV-08
40401|Mirage Granite|73155|5|Briefly described|p266-267, p275, p277, p282 Fig.13, p283|||Mount Woods Domain, central. Informal name. Moderately magnetic with stippled magnetic texture. Syn-tectonic, overprinted by NE-trending faults. Interpreted as part of basement rocks in footwall/lower plate of Mount Woods Metamorphic Core Complex. See also p268-269 Fig.3, p273.||Mount Woods Metamorphics||Intrudes Mount Woods Metamorphics.|Includes medium-grained, porphyritic to megacrystic quartz, K-feldspar, biotite +/- garnet granitic gneiss to mylonite, elongated K-feldspar porphyroclasts define a very well developed mineral lineation within the orthogneiss.|
29823|Mobella Tonalite|24472|5|Briefly described|p5 Tb.1|Archean|Archean|Geological Province: Harris Greenstone Domain, Gawler Craton. Age: ~2458 Ma (Rb-Sr). Parent: Mulgathing Complex.||||||07-NOV-08
29823|Mobella Tonalite|43052|4|Described|p43, Table 3.2|||Of Mulgathing Complex||||||
29823|Mobella Tonalite|50605|5|Briefly described|p8.7|||Of the Mulgathing Complex. Geological Province: Gawler Craton & Curnamona Province.||||||06-MAY-16
29823|Mobella Tonalite|60953|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Synorogenic tonalite, minor granite and adamellite.||||||07-NOV-08
29823|Mobella Tonalite|61108|5|Briefly described|map legend||Archean|Synorogenic tonalite, minor granite and adamellite.||||||07-NOV-08
29823|Mobella Tonalite|65376|6|Mentioned|p190.|||||Unit in Mulgathing Complex.||||
29823|Mobella Tonalite|65385|5|Briefly described|pS132|Siderian|Siderian|Of Mulgathing Complex. Synorogenic magmatism. ~2460 Ma.||||||08-MAR-12
29823|Mobella Tonalite|65915|6|Mentioned|p3 Fig.2, p18|||A single inherited zircon was identified with an age of ~3500 Ma, suggesting Paleoarchean crust is present below its emplacement level in the Mulgathing Complex.||||||
29823|Mobella Tonalite|66302|6|Mentioned|p12|||Christie and Wilgena Domains, Gawler Craton. Ages are SHRIMP U-Pb from Jagodzinski et al. (2009). |2496 +/- 4 Ma to 2490 +/- 4 Ma |||||
29823|Mobella Tonalite|68128|5|Briefly described|p2-p3, p5, p43, p71-72, |Palaeoproterozoic||Gawler Craton. An additional SHRIMP age of 2488 +/- 6 Ma is provided. A Rb-Sr age is derived from Webb, 1978 and is 2458 +/- 60 Ma. Petrography, zircon description, SHRIMP analyses and results are discussed. See also p75-77, p79-81, p109.|2493 +/- 6 Ma (SHRIMP)|Mulgathing Complex|||Tonalite, grey, coarse-grained, weakly foliated.|31-JAN-23
29823|Mobella Tonalite|68208|6|Mentioned|p31 Fig.2|Paleoproterozoic|Paleoproterozoic||Crystallisation age ~2488 Ma|Of Mulgathing Complex||||
29823|Mobella Tonalite|73230|5|Briefly described|p6, p9-10, p14|Siderian|Siderian|Gawler Craton. Domain: Christie and Wilgena. Temporal correlative of the Burden Metagabbro.|c. 2490 Ma (magmatic)|Mulgathing Complex||Intrudes Christie Gneiss.|Grey, coarse-grained, poorly foliated tonalite-quartz monzonite.|
39176|Mona Volcanics Member|24475|2|Defined|p54|Paleoproterozoic|Paleoproterozoic|Of Weetulta Formation.  Includes two contrasting lithologies.||||||07-NOV-08
39176|Mona Volcanics Member|65375|6|Mentioned|p19, p22.|||Felsics in the Bute area.||Unit in Weetulta Formation.||||
39176|Mona Volcanics Member|65376|5|Briefly described|pp106-109. ||||1740 +/- 16 Ma to 1735 +/- 10 Ma.|Unit in Weetulta Formation.||Intercalated with the Wokurna Member in the Bute region.|Dacitic to rhyodacitic porphyry, and fine-bedded tuffaceous siltstone.|
39176|Mona Volcanics Member|66302|5|Briefly described|p29, p33|Statherian|Statherian|Olympic Domain, Gawler Craton. Ages are derived from Fanning et al. (2007).|1735 +/- 10 Ma and 1740 +/- 16 Ma |Weetulta Formation||||
39176|Mona Volcanics Member|73155|6|Mentioned|p281 Fig.12|||||Wallaroo Group||||
26036|Monash Formation|22495|6|Mentioned|P220|||||||||
26036|Monash Formation|22773|5|Briefly described|Fig24.5p350|Early Cretaceous|Early Cretaceous|Consists of: Coombool Member, Merreti Member and Pyap Member.||||||
26036|Monash Formation|22799|2|Defined|p18|Albian|Aptian|||||||
26036|Monash Formation|22857|5|Briefly described|p318, p548 App.1 Tb.A1.12|||Max. thickness: 279m in type area in SA. Geological Province: Berri Basin. See also p350 Fig.24.5.||||||
26036|Monash Formation|22865|6|Mentioned|p318|||(Thornton 1972).||||||
26036|Monash Formation|22887|4|Described|p30, Table 5 p31|Early Cretaceous|Early Cretaceous|See also Fig.5 p12. Renmark Trough.||||||
26036|Monash Formation|22893|6|Mentioned|table5 fig4||Early Cretaceous|||||||
26036|Monash Formation|23836|4|Described|p93|Cretaceous|Cretaceous|Geological Province: Murray Basin.||||||
26036|Monash Formation|24551|5|Briefly described|p270|||Geological Province: Murray Basin.||||||
26036|Monash Formation|33488|2|Defined|p8|Early Cretaceous|Early Cretaceous|See also PP9-11||||||
26036|Monash Formation|33490|4|Described|p10|||Cretaceous. See also P23||||||
26036|Monash Formation|35200|6|Mentioned|Map legend|Mesozoic|Mesozoic|||||||
26036|Monash Formation|35232|6|Mentioned|Table.2|||||||||
26036|Monash Formation|39211|6|Mentioned|Fig.23|||||||||
26036|Monash Formation|42133|6|Mentioned|Fig.7 P315|||||||||
26036|Monash Formation|42966|2|Defined|p71|Albian|Aptian|||||||
26036|Monash Formation|43052|5|Briefly described|Table 2.1|||||||||
26036|Monash Formation|43218|4|Described|Fig.3,p22|Albian|Aptian|||||||
26036|Monash Formation|44133|5|Briefly described|p94, 127|Cretaceous|Cretaceous|Geological Province: Berri Basin. Unconformably overlies Urana Formation. Unconformably overlain by Renmark Group. ||||||
26036|Monash Formation|44191|5|Briefly described|Map Legend||Early Cretaceous|||||||
26036|Monash Formation|49038|5|Briefly described|p23|||||||||
26036|Monash Formation|49040|6|Mentioned|p8|||||||||
26036|Monash Formation|61314|5|Briefly described|p129|Early Cretaceous|Early Cretaceous|Comprises three sequences of strata: the Pyap, Merreti and Coombool Members. Geological Province: western Murray Basin.||||||
26036|Monash Formation|68189|6|Mentioned|p25|||Of the Murray Basin.|||Includes the Coombool Member.|||
26036|Monash Formation|68715|6|Mentioned|p31 Fig.5|Albian|Aptian|Berri Basin.||||||
26036|Monash Formation|73228|6|Mentioned|p50-54|Early Cretaceous|Early Cretaceous|Berri Basin. Identified in Cooltong 1, Berri North 1, Nadda 1, Loxton 1, and Overland Corner 1 drillholes. Type section is subsurface in North Renmark 1 (Thornton, 1972).|||Coombool Member, Merreti Member, Pyap Member|Unconformably underlain by Urana Formation. Overlain by Warina Sand, Renmark Group.||
26036|Monash Formation|73229|6|Mentioned|p66-68|Early Cretaceous|Early Cretaceous|Berri Basin.|||Coombool Member, Merreti Member, and Pyap Member|||
26747|Montacute Dolomite|9124|6|Mentioned|Map Legend|Adelaidean|Adelaidean|||||||
26747|Montacute Dolomite|22869|6|Mentioned|p38|||||||||07-NOV-22
26747|Montacute Dolomite|22889|5|Briefly described|p34|Adelaidean|Adelaidean|Parent - Mundallio Subgroup.||||||
26747|Montacute Dolomite|23818|4|Described|p59|Adelaidean|Adelaidean|Geological Province: Adelaide Geosyncline. Of the Skillogalee Dolomite. Max. thickness: >5000 ft (in some areas).||||||
26747|Montacute Dolomite|29776|6|Mentioned|p82|||||||||
26747|Montacute Dolomite|32417|6|Mentioned|p3|||Breccias in||||||
26747|Montacute Dolomite|32724|6|Mentioned|Fig.1|||Torrensian. Correlation||||||
26747|Montacute Dolomite|33224|6|Mentioned|Fig.34|||Photo||||||
26747|Montacute Dolomite|33547|6|Mentioned|Fig.6|||||||||
26747|Montacute Dolomite|34483|6|Mentioned|p113|||Late Precambrian||||||
26747|Montacute Dolomite|34535|6|Mentioned|p59|||Early Torrensian||||||
26747|Montacute Dolomite|35003|6|Mentioned|p122|||||||||
26747|Montacute Dolomite|35354|6|Mentioned|p46|||||||||
26747|Montacute Dolomite|37461|6|Mentioned|Table 5.I|||||||||
26747|Montacute Dolomite|38157|6|Mentioned|Table III|||||||||
26747|Montacute Dolomite|38926|4|Described|p26|||||||||
26747|Montacute Dolomite|39350|6|Mentioned|Map legend|Adelaidean|Adelaidean|Torrensian||||||
26747|Montacute Dolomite|40003|6|Mentioned|Table 16|||||||||
26747|Montacute Dolomite|40294|6|Mentioned|Table 2|||||||||
26747|Montacute Dolomite|40442|5|Briefly described|p8|||See also Fig.4.||||||
26747|Montacute Dolomite|41404|4|Described|p98|||||||||
26747|Montacute Dolomite|41526|6|Mentioned|p50|||||||||
26747|Montacute Dolomite|42093|5|Briefly described|p6|||See also Fig.2||||||
26747|Montacute Dolomite|42222|6|Mentioned|p14|||||||||
26747|Montacute Dolomite|42236|5|Briefly described|p107|||See also Fig.2||||||
26747|Montacute Dolomite|42733|5|Briefly described|map legend|Adelaidean||||||||
26747|Montacute Dolomite|43052|5|Briefly described|p179,Table 6.1|||Of Mundallio Subgroup.||||||03-FEB-09
26747|Montacute Dolomite|50615|5|Briefly described|p303 Fig. 2, p306 Fig. 4|||Geological Province: Adelaide Fold Belt. See also p304 Fig. 3.||||||
26747|Montacute Dolomite|64647|6|Mentioned|p39 Fig. 2, p40|Neoproterozoic|Neoproterozoic|Of Burra Group. Calcsilicate.||||||
26747|Montacute Dolomite|71237|14|Not recorded|p9|||||||||
26747|Montacute Dolomite|71240|14|Not recorded|p6, p9|||||||Correlated with Skillogalee Dolomite.||
26747|Montacute Dolomite|72450|6|Mentioned|Brochure|||Together with the Aldgate Sandstone are the oldest sedimentary rocks deposited on the Barossa Complex basement. Overlain by a number of younger rocks including siltstone, sandstone and quartzite units. Deformed by the Delamerian Orogeny.||||||
26747|Montacute Dolomite|73188|5|Briefly described|p316, p324, p327|Neoproterozoic|Neoproterozoic|Mount Lofty Ranges.||Mundallio Subgroup, Burra Group|||Dark grey dolomite, sedimentary magnesite, sandstone, chert.|
80053|Montstephen Subsuite|70405|4|Described|p36|Paleoproterozoic|Paleoproterozoic|Formerly known as 'Montstephen Metabasalt' and informally as the 'Weekeroo amphibolite'.|1710 Ma - 1720 Ma|Bumbumbie Suite||Intrudes Bewooloo Member|Mafic pillow lavas. Metabasalt is partly amygdaloidal and is closely associated with exhalative deposits. Volcaniclastic breccia (mafics).|21-SEP-17
79174|Moodini Supersuite|70748|6|Mentioned|p50|Stenian|Stenian|Madura Province. Similar in age to the Eyre 1 granite.|c. 1180-1125 Ma (Wingate et al, 2015b)|||||
79174|Moodini Supersuite|70802|5|Briefly described|250k_pre_mesozoic_interpgeop_lut.csv|Mesoproterozoic|Mesoproterozoic|Geological province: Coompana Province; Madura Province. Events: Maralinga Event (1200-1100 Ma); Albany-Fraser Orogeny Stage II (1225-1140 Ma); Musgrave Orogeny (1220-1150 Ma); Coompana Province events (2500-1200 Ma).|1200-1100 Ma (inferred)||||Dominantly gabbroic rocks; may include leucogabbro, granite, and inclusions of basalt|
79174|Moodini Supersuite|70813|6|Mentioned|p5|||Albany-Fraser Orogen.||||||
79174|Moodini Supersuite|70831|5|Briefly described|p26|Stenian|Stenian|Madura Province.|c. 1192-1130 Ma|||||
79174|Moodini Supersuite|71143|5|Briefly described|p427,429,431,433-438|Stenian|Stenian|Geological province: Madura and Coompana provinces. Contains juvenile isotopic signatures interpreted to reflect mixed mafic lower-crustal and asthenospheric melts produced at the base of thinned crust. Comprises three main magmatic groups; 1192-1150Ma crustal melts (western Coompana Province), 1181-1125 high-KFe mafic to granitic intrusions (Madura Province) and the 1192-1180 Ma Bottle Corner Shoshonite (western Coompana Province). |1192-1125 Ma||Includes Bottle Corner Shoshonite.|||
79174|Moodini Supersuite|71165|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic||||Bottle Corner Shoshonite, Kestral Cavern Gabbro.|Intrudes Undawidgi Supersuite.|Granitic and gabbroic rocks.|25-JUN-17
79174|Moodini Supersuite|71618|6|Mentioned|p135|Mesoproterozoic|Mesoproterozoic|Geological province: Madura and Coompana provinces. Possible source of c. 1150 (~1000-1300) Ma zircon in Shanes Dam Conglomerate.||||||
79174|Moodini Supersuite|71891|5|Briefly described|p8, p32, p44-p46|||Coompana Province.|||||Equigranular to porphyritic, massive syenogranites, shoshonites and monzogranites.|
79174|Moodini Supersuite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoproterozoic|Mesoproterozoic|Coompana Province; Madura Province.|||||Granitic and gabbroic rocks; typically undeformed.|30-NOV-21
79174|Moodini Supersuite|72059|5|Briefly described|p57|Stenian|Stenian|Geological province: Fraser Zone, Albany-Fraser Orogen. Magmatism associated with Stage II (1225-1140 Ma) Albany-Fraser Orogeny.||||||
79174|Moodini Supersuite|72242|5|Briefly described|p27,29-30|Stenian|Stenian|Geological province: Madura and Musgrave provinces. Bimodal magmatism associated with Maralinga Event (including Musgrave Orogeny). Coeval with Pitjantjatjara Supersuite.|c. 1200-1120||Includes Koonalda Supersuite.|||
79174|Moodini Supersuite|72344|5|Briefly described|p3, p5, p7-p9, p23, p28, p49-p50, p54|Stenian|Stenian|Coompana Province. Intersected in drillhole CDP001 where magmatic crystallisation was dated via SHRIMP at 1141 +/- 15 Ma (present volume). An additional magmatic age of 1148 +/- 7 Ma is derived from this volume via SHRIMP. Petrography, SHRIMP analyses and geochemistry are discussed for several samples. See also p76, p84, p102, p143, p160.|c. 1191-1140 Ma||Includes the Koonalda Suite.||High-K-Mg shoshonitic magmas that are bimodal; includes equigranular to porphyritic, massive syenogranites, shoshonites and monzogranites that form thin sheets.|
79174|Moodini Supersuite|72465|5|Briefly described|p4, 10|||Coompana Province. Crustal thinning and reworking produced widespread intra-plate intrusions. The text also gives an age range of c.1190-1140 Ma.|1168 +/- 6 Ma to 1140 +/- 8 Ma.||||Thin sheets of equigranular to porphyritic, massive syenogranites, shoshonites and monzogranites.|
79174|Moodini Supersuite|72466|5|Briefly described|p4, 10|||Spaggiari and Smithies (2015). Basement to western Coompana Province. Reflects deep melting of wet, oxidised modified mantle lithosphere and widespread reworking of the crust.|1613/- 13 Ma to 1591 +/- 11 Ma.||||Includes equigranular to porphyritic, massive syenogranites, shoshonites and monzogranites that form thin sheets.|
79174|Moodini Supersuite|72467|5|Briefly described|p4, 10, 17|||Coompana Province. Crustal thinning and reworking produced widespread intra-plate intrusions. The text also gives an age range of c.1190-1140 Ma.|1168 +/- 6 Ma to 1140 +/- 8 Ma.||||Thin sheets of equigranular to porphyritic, massive syenogranites, shoshonites and monzogranites.|
79174|Moodini Supersuite|72468|5|Briefly described|p4, p10|Stenian|Stenian|Coompana Province. Represents widespread intraplate magmatism. May represent a MASH zone. Magmatic ages of 1168 +/- 6 Ma and 1140 +/- 8 Ma.|c. 1190-1140 Ma||||Bimodal shoshonitic rocks including equigranular to porphyritic, massive syenogranites, shoshonites and monzogranites.|
79174|Moodini Supersuite|72469|5|Briefly described|p4, p10, p17|Stenian|Stenian|Coompana Province. Represents widespread intraplate magmatism. May represent a MASH zone. Magmatic ages of 1168 +/- 6 Ma and 1140 +/- 8 Ma.|c. 1190-1140 Ma||||Bimodal shoshonitic rocks including equigranular to porphyritic, massive syenogranites, shoshonites and monzogranites.|
79174|Moodini Supersuite|72470|5|Briefly described|p4, p10, p24|Stenian|Stenian|Coompana Province. Represents widespread intraplate magmatism. May represent a MASH zone. Magmatic ages of 1168 +/- 6 Ma and 1140 +/- 8 Ma.|c. 1190-1140 Ma||||Bimodal shoshonitic rocks including equigranular to porphyritic, massive syenogranites, shoshonites and monzogranites.|
79174|Moodini Supersuite|72471|5|Briefly described|p4, p10|Stenian|Stenian|Coompana Province. Represents widespread intraplate magmatism. May represent a MASH zone. Magmatic ages of 1168 +/- 6 Ma and 1140 +/- 8 Ma.|c. 1190-1140 Ma||||Bimodal shoshonitic rocks including equigranular to porphyritic, massive syenogranites, shoshonites and monzogranites.|
79174|Moodini Supersuite|72472|5|Briefly described|p4, p10|Stenian|Stenian|Coompana Province. Represents widespread intraplate magmatism. May represent a MASH zone. Magmatic ages of 1168 +/- 6 Ma and 1140 +/- 8 Ma.|c. 1190-1140 Ma||||Bimodal shoshonitic rocks including equigranular to porphyritic, massive syenogranites, shoshonites and monzogranites.|
79174|Moodini Supersuite|72710|6|Mentioned|p4.|Stenian|Stenian|This supersuite intrudes into both the Coompana and Madura.|1192 Ma to 1127 Ma.||||Includes granitic rocks.|
79174|Moodini Supersuite|72934|5|Briefly described|p2, p4, p11-13, App.A|Stenian|Stenian|Intrude the western part of the Coompana Province. Appears to be part of a much larger crustal reworking event that followed convergence of the South, West and North Australian Cratons. Yielded U-Pb SIMS zircon magmatic crystallisation ages of 1198 +/- 11 Ma, 1174 +/- 9 Ma, 1150 +/- 5 Ma, and 1141 +/- 15 Ma; and inheritance ages of 1527 +/- 6 Ma and 1622 +/- 14 Ma.|1192-1125 Ma||||High-K, Mg shoshonitic mafic to granitic plutons with lesser high-K, Fe A-type rocks.|
79174|Moodini Supersuite|72947|5|Briefly described|p4, p7-9, p14, p16|Stenian|Stenian|Coompana Province. Represents extension and partial melting of the crust. Part of a broader tectonomagmatic event between the West, South and North Australian cratons, affecting the Musgrave Province to the north, and the Madura Province and Albany-Fraser Orogen to the west.|[c.] 1192 - [1150/1141/1140] Ma||Merdayerrah Shoshonite, Koonalda Suite, Albala-Karoo Syenogranite|||29-NOV-22
79174|Moodini Supersuite|73084|4|Described|p: 12, 15, 21, 24, 28, 39, 45, 54, 56...|Stenian|Stenian|Madura and Coompana Provinces. Part of a regionally extensive, high-temperature event named the Maralinga Event by Spaggiari et al. (2016). Compositionally similar and broadly contemporaneous with Pitjantjatjara Supersuite of the Musgrave Province and Esperance Supersuite, particularly Booanya Suite, of the Albany-Fraser Orogen. Dominates much of the Madura Province (intrusions between 1182-1127 Ma). Regionally extensive and slightly older in the Coompana Province (1192-1140 Ma). Report includes lithologic/petrographic description, structural analysis, whole-rock geochemistry, geochronology, Sm-Nd, Lu-Hf. [an informal monzonite from the unit is referred to by a location name; not interpreted to reflect a specific lithologic unit; i.e., Hannah]. Also p: 63, 69-73, 79, 81, 84, 89, ~94-118, ~123-142.|1192-1127 Ma||Kestrel Cavern Gabbro, Bottle Corner Shoshonite, Koonalda Suite||Ferrogabbroic to granitic rocks including shoshonite, granite, pegmatite, mozogranite, granodiorite.|
79174|Moodini Supersuite|73091|5|Briefly described|map legend|Stenian|Stenian||c. 1200-1120 Ma||Includes the Koonalda Suite.||Felsic intrusives.|30-NOV-21
79174|Moodini Supersuite|73224|6|Mentioned|p42, p44|Stenian|Stenian||c. 1181-1125 Ma||Konalda Suite|||
79174|Moodini Supersuite|73225|5|Briefly described|p2, 4, 11, 18|||Madura Province. West of Mulyawarra Shear Zone. Represents low-medium-P melts of mafic crust. Appears as Moodini Suite on p11. Age range also given as c.1192-1175 Ma.|1181-1125 Ma.||Koonalda Suite; Bottle Corner Shoshonite.||High K-Fe rocks; granites.|
79174|Moodini Supersuite|73641|5|Briefly described|p2, 4||||1175-1140 Ma||Koonalda Suite|Is intruded by Giants Head Suite.|Extensive mafic-felsic magmatism.|
28766|Moodlatana Formation|22766|5|Briefly described|Fig.2 p561, 562, 566|Middle Cambrian|Early Cambrian|||||||
28766|Moodlatana Formation|22857|5|Briefly described|p90 Fig. 14.7B|Late Cambrian|Late Cambrian|Of the Lake Frome Group. Geological Province: Arrowie Basin.||||||
28766|Moodlatana Formation|22858|6|Mentioned|Fig14.7bp90-1|||||||||
28766|Moodlatana Formation|23282|6|Mentioned|p79|||Interpreted equivalent of Trainor Hill Sandstone. of Arrowie Basin.||||||
28766|Moodlatana Formation|23818|5|Briefly described|p87 Fig.33|Cambrian|Cambrian|Oldest formation of the Lake Frome Group.||||||
28766|Moodlatana Formation|24072|5|Briefly described|p369 Fig.1|Cambrian|Cambrian|Geological Province: Great Artesian Basin.||||||
28766|Moodlatana Formation|24176|4|Described|p17, p23 Tb. 1|Late Cambrian|Late Cambrian|Red-brown sandstone, minor calcareous siltstone and sandstone. Of the Lake Frome Group. Overlain by Balcoracana Formation. Max. thickness: 165m.  Geological Province: Mount Painter Province.||||||23-JUN-09
28766|Moodlatana Formation|24465|5|Briefly described|p345 Fig.2|Middle Cambrian|Early Cambrian|Of Lake Frome Group.  Geological Province: Arrowie Basin.||||||19-JAN-05
28766|Moodlatana Formation|24484|5|Briefly described|p798 Fig. 1|Cambrian|Cambrian|Overlies the Aroona Creek Limestone.||||||
28766|Moodlatana Formation|30051|6|Mentioned|Fig.4|||||||||
28766|Moodlatana Formation|30176|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
28766|Moodlatana Formation|30801|6|Mentioned|p5|||Lake Frome Group. Table P5-6||||||
28766|Moodlatana Formation|30802|5|Briefly described|p11|||Cambrian age||||||
28766|Moodlatana Formation|30807|6|Mentioned|p102|||Suggested map symbol||||||
28766|Moodlatana Formation|31539|6|Mentioned|Fig. 28|||||||||
28766|Moodlatana Formation|31706|6|Mentioned|p633|||Cambrian correlation chart||||||
28766|Moodlatana Formation|33474|6|Mentioned|Fig.3|||||||||
28766|Moodlatana Formation|33932|6|Mentioned|Fig.2|||||||||
28766|Moodlatana Formation|33934|6|Mentioned|Fig.2|||M - U Camb.||||||
28766|Moodlatana Formation|33972|6|Mentioned|Plate 14|||||||||
28766|Moodlatana Formation|33973|6|Mentioned|Fig.2|||||||||
28766|Moodlatana Formation|34269|6|Mentioned|Table 1|||||||||
28766|Moodlatana Formation|34610|6|Mentioned|p178|||Lake Frome Group||||||
28766|Moodlatana Formation|34612|6|Mentioned|p95|||See also correlation chart. Fig.33||||||
28766|Moodlatana Formation|35255|6|Mentioned|Fig.8|||See also P43.||||||
28766|Moodlatana Formation|35835|6|Mentioned|p198|||||||||
28766|Moodlatana Formation|36083|5|Briefly described|p473|||||||||
28766|Moodlatana Formation|36198|6|Mentioned|Fig.I.2|||||||||
28766|Moodlatana Formation|36525|6|Mentioned|Fig.4|||||||||
28766|Moodlatana Formation|38329|6|Mentioned|p202|||||||||
28766|Moodlatana Formation|40852|6|Mentioned|Fig.3.7|||||||||
28766|Moodlatana Formation|40856|6|Mentioned|Fig.23.6|||||||||
28766|Moodlatana Formation|40914|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
28766|Moodlatana Formation|42225|6|Mentioned|Fig.4 P224|||||||||
28766|Moodlatana Formation|42269|5|Briefly described|p337|||||||||
28766|Moodlatana Formation|42272|6|Mentioned|p414|||||||||
28766|Moodlatana Formation|42440|6|Mentioned|Fig.2 P602|||||||||
28766|Moodlatana Formation|43781|6|Mentioned|p4|||||||||
28766|Moodlatana Formation|43845|6|Mentioned|Fig4 p44|||||||||12-JUL-16
28766|Moodlatana Formation|44133|5|Briefly described|p4 Fig. 7.2, 5, 28|Middle Cambrian|Early Cambrian|Geological Province: Arrowie Basin.||||||
28766|Moodlatana Formation|60418|5|Briefly described|p134 Fig.1|Cambrian|Cambrian|Of Lake Frome Group.||||||
28766|Moodlatana Formation|60889|4|Described|p245 Fig.2, p247 Fig.4, p249, p251-254|Early Cambrian|Early Cambrian|Marginal marine lowstand deposits. Thickness: 400 m. Arrowie Basin. Shown as Moodlatana Fm. Traces of free oil recorded, no flow on DST (Moorowie-1).||Lake Frome Group||Overlies Wirrealpa Limestone (unconformably?). Is overlain by Balcoracana Formation.|Shale, siltstone with evaporite casts and cross-bedded fine to medium sandstone with minor carbonates.|
28766|Moodlatana Formation|60959|5|Briefly described|Map Legend|Middle Cambrian|Early Cambrian|Of the Lake Frome Group. Micaceous siltstone, shale, sandstone, carbonate.||||||
28766|Moodlatana Formation|62592|5|Briefly described|p50 Table 5.1.|Early Cambrian|Early Cambrian|Adelaide Geosyncline.||Unit in Lake Frome Group.||Is overlain by Balcoracana Formation.|Redbeds.|
28766|Moodlatana Formation|62784|5|Briefly described|p8 Fig.1|Cambrian|Cambrian|Arrowie Basin. Unit of Lake Frome Group. Overlies Wirrealpa Limestone.||||||
28766|Moodlatana Formation|62787|6|Mentioned|p82 Fig. 3|Cambrian|Cambrian|Geological Province: Arrowie Basin (SA).||||||07-FEB-11
28766|Moodlatana Formation|63569|5|Briefly described|p117, p119-120, p122|Early Cambrian|Early Cambrian|Arrowie Basin. Thickness 400 m.||Unit in Lake Frome Group.||Overlies Wirrealpa Limestone.|Micaceous shales, siltstone and sandstone; red beds.|
28766|Moodlatana Formation|64829|5|Briefly described|p1084-5 Figs.1,  2|Middle Cambrian|Early Cambrian|Unit discussed in the context of soilscapes and palaeosols. First appearance of the trilobite, Onaraspis rubra. Geological province: Arrowie Basin. Has associated palaeosols.||||||07-FEB-11
28766|Moodlatana Formation|65313|5|Briefly described|p576, 577, p578 Fig. 6, Fig. 2, p 573|Middle Cambrian|Middle Cambrian|Age based on trilobite Onaraspis rubra. Shown as Arcadian age in Fig. 6.|ca 510 Ma.|Of Lake Frome Group.||Overlies Wirrealpa Limestone, underlies Balcoracana Formation.||26-MAR-12
28766|Moodlatana Formation|65375|5|Briefly described|p33.|Early Cambrian|Early Cambrian|||Unit in Lake Frome Group.||Overlies Wirrealpa Limestone. Is overlain by Balcoracana Formation.||
28766|Moodlatana Formation|65625|5|Briefly described|p103 Fig.2|Middle Cambrian|Middle Cambrian|Lake Frome area.||Of Lake Frome Group.||Overlies Wirrealpa Limestone. Overlain by Balcoracana Formation.||16-FEB-11
28766|Moodlatana Formation|65686|5|Briefly described|p411,  p409 Fig 2|Early Cambrian|Early Cambrian|Arrowie Basin, 400m thick.||||||
28766|Moodlatana Formation|65892|5|Briefly described|p7 Fig.3, p9 Fig.4, p11, p12, p41, p48. |Early Cambrian|Early Cambrian|Arrowie Basin. 400m thick. Contains metadoxidid Onaraspis rubra. Marginal marine lowstand deposits. Mud cracks, evaporite casts and trilobite tracks are abundant.||Unit in Lake Frome Group.||Overlies Wirrealpa Limestone. Is overlain by Balcoracana Formation.|Shale, siltstone with evaporite casts, cross-bedded fine to medium red sandstone; minor carbonates.|
28766|Moodlatana Formation|65925|5|Briefly described|p14 Fig.2.2, Appendix 2.|Early Cambrian|Early Cambrian|||Unit in Lake Frome Group.|||Micaceous siltstone, shale, arkosic fine- to medium-grained sandstone; minor carbonate.|
28766|Moodlatana Formation|66518|6|Mentioned|p19 Fig.4.|Cambrian|Cambrian|Arrowie Basin. ||Unit in Lake Frome Group.||Overlies Wirrealpa Limestone and is overlain by Balcoracana Formation.||
28766|Moodlatana Formation|68735|4|Described|pp233-238|Early Cambrian|Early Cambrian|Arrowie Basin. ~ 400 m thick. Two or three thin carbonate units occur at the top of this formation. Some cryptomicrobial laminations contain the youngest known trilobite fossils in the Flinders Ranges - Onaraspis rubra (Jell, in Bengtson et al. 1990). Cross-bedding rose diagrams.||Bottom unit of the Lake Frome Group.||Overlain by the Balcoracana Formation.|Comprises marginal marine red cross-bedded sandstones, siltstones, and shales that have abundant trace fossils and evaporite clasts.|10-APR-17
28766|Moodlatana Formation|68993|5|Briefly described|p543, p544 Fig.1|Early Cambrian|Early Cambrian|Arrowie Basin. Contains the trilobite Onaraspis rubra within the top part of this unit (Jell in Bengtston et al. 1990); correlation with the latest Toyonian of Siberia was suggested by Geyer and Shergold (2000) and Patterson and Brock (2007).||Of the Lake Frome Group.||||
28766|Moodlatana Formation|69570|6|Mentioned|p421 fig 1|Cambrian|Cambrian|Arrowie Syncline, Flinder Ranges.||||||
28766|Moodlatana Formation|70835|6|Mentioned|p335|Cambrian|Cambrian|Arrowie Basin, Flinders Ranges.||Lake Frome Group.||||
28766|Moodlatana Formation|72449|5|Briefly described|p2 Map Legend|Cambrian|Cambrian|||||Overlies Wirrealpa Limestone and underlies Balcoracana Formation.|Mica-rich siltstone, shale and white, fine to medium-grained sandstone, planar to ripple-bedded or cross-bedded, with mudcracks, salt casts and trilobite tracks.|
28766|Moodlatana Formation|73251|6|Mentioned|p36|Cambrian|Cambrian|Arrowie Basin, Moorowie and Yalkalpo Sub-basins. Thermally late to post-mature.||Lake Frome Group||Underlain by Wirrealpa Limestone. Overlain by Balcoracana Formation.||
28766|Moodlatana Formation|73255|6|Mentioned|p534 Fig.2|Cambrian|early Cambrian|Contains Onarapsis rubra trilobite  fossils. Minumum age of mid- to late-Cambrian||||Overlies the Wirrealpa Limestone, underlies the Balcoracana Formation.||
27839|Moody Suite|22489|5|Briefly described|p12|||||||||
27839|Moody Suite|22629|6|Mentioned|p157|Statherian|Statherian|Age: 1700Ma||||||
27839|Moody Suite|22834|2|Defined|P39||Statherian|Intrudes Hutchison Group and Sleaford Complex.||||||21-OCT-08
27839|Moody Suite|23285|5|Briefly described|p 334|||||||||
27839|Moody Suite|23791|6|Mentioned|p5 Fig. 4|||See also Moody Granitoid Suite.||||||
27839|Moody Suite|23803|6|Mentioned|p29|||Geological Province: Gawler Craton.||||||
27839|Moody Suite|24505|5|Briefly described|p5 Fig. 1|||Geological Province: Gawler Craton.||||||15-SEP-05
27839|Moody Suite|24508|5|Briefly described|p30|||Intrusive monzogranites to leucogranites.  Geological Province: Gawler Craton.||||||
27839|Moody Suite|24522|6|Mentioned|p82|Paleoproterozoic|Paleoproterozoic|Age: 1.74-1.70Ga (Daly et al 1998; Hoek and Schaefer 1998).||||||07-NOV-08
27839|Moody Suite|40448|5|Briefly described|p35 Table 4||||1677+/-125Ma, 1655+/-61Ma, 1601+/-14Ma|Of Lincoln Complex|Includes Wertigo Granite, Carpa Granite, Burkitt Granite.|||12-AUG-10
27839|Moody Suite|40644|6|Mentioned|p133, p134 Tb. 3|Paleoproterozoic|Paleoproterozoic|Granites near Tumby Bay. Age: 1650-1600Ma; although an age of 1740Ma (Rb-Sr) has also been determined. Also presented as the informal Moody suite.||||||02-JUN-09
27839|Moody Suite|41667|4|Described|p11|||||||||
27839|Moody Suite|41682|6|Mentioned|p14|||||||||
27839|Moody Suite|41972|6|Mentioned|Fig.3 P366|||||||||
27839|Moody Suite|43052|4|Described|p81,Table 4.4|||Of the Lincoln Complex.||||||18-JAN-07
27839|Moody Suite|50605|5|Briefly described|p3.1, 5.2|||Of the Younger Lincoln Supersuite. Geological Province: Gawler Craton and Curnamona Province.||||||18-JAN-07
27839|Moody Suite|60515|6|Mentioned|p116 Fig.1 |||||||||
27839|Moody Suite|60534|5|Briefly described|p572 Fig.1, 573 Fig.2|Paleoproterozoic|Paleoproterozoic|Age: 1700-1750 Ma. Geological Province: Gawler Craton.||||||07-NOV-08
27839|Moody Suite|60704|5|Briefly described|p686 Fig.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Gawler Craton (Kimban Orogeny). Possibly equivalent to the Paxton Granite.||||||07-NOV-08
27839|Moody Suite|60953|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Age: 1702-1690Ma. Late tectonic granitoids.||||||07-NOV-08
27839|Moody Suite|61070|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Undifferentiated granitoids. Typically weakly to moderately foliated. Includes I-type intermediate and S-type felsic intrusives, variably deformed and metamorphosed. Geological Province: Gawler Craton.||||||12-JAN-10
27839|Moody Suite|61108|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|Late tectonic granite to granodiorite. Age: 1702-1690 Ma.||||||07-NOV-08
27839|Moody Suite|61262|5|Briefly described|p455 Fig. 11|Paleoproterozoic|Paleoproterozoic|Age: ~1700Ma. Geological Province: eastern Gawler Craton.||||||07-NOV-08
27839|Moody Suite|61307|5|Briefly described|p39 Fig. 19|Paleoproterozoic|Paleoproterozoic|Abbreviated version of Moody Granitoid Suite. Geological Province: Gawler Craton. ||||||07-NOV-08
27839|Moody Suite|61522|5|Briefly described|p5 Fig.1|||Geological Province: Gawler Craton.||||||
27839|Moody Suite|63020|5|Briefly described|p983, p987 Fig. 8|Paleoproterozoic|Paleoproterozoic|Felsic intrusion. Age: 1702+/-10Ma. Geological Province: Gawler Craton (Spencer Domain).||||||07-NOV-08
27839|Moody Suite|63866|5|Briefly described|p6, p9, p18-p20, p31|Statherian|Statherian|Cleve, Coulta and Spencer Domains, Gawler Craton. A SHRIMP U-Pb zircon age of magmatic crystallisation, dated at 1710 +/- 11 Ma is generally consistent with intrusions of this suite.|c. 1710-1700 Ma||||Granites.|
27839|Moody Suite|64130|5|Briefly described|p1378 Fig.1, p1380 Fig.2, p1381-1382|Paleoproterozoic|Paleoproterozoic|Southern Gawler Craton. Syn-Kimban Orogeny. Consists of I-type intermediate and S-type felsic rocks.|c.1730-c.1710 Ma (Fanning et al., 2007).|||Intrudes Hutchison Group and Sleaford Complex.||
27839|Moody Suite|64137|5|Briefly described|p1542 Fig.1, p1544|Paleoproterozoic|Paleoproterozoic|~1700 Ma (Ferris et al., 2002)||||||
27839|Moody Suite|64313|5|Briefly described|p450 Fig. 1|Paleoproterozoic|Paleoproterozoic|Age: ~1700Ma. Geological province: Gawler Craton. See also p451 Fig.2b.||||||09-FEB-10
27839|Moody Suite|64576|6|Mentioned|p625 Fig. 2|Paleoproterozoic|Paleoproterozoic|Age: c. 1700Ma.||||||
27839|Moody Suite|64722|6|Mentioned|p14|Statherian|Statherian|A product of extensive granite magmatism in the Gawler Province that occurred mainly between 1690-1670 Ma.||||||11-APR-12
27839|Moody Suite|64725|6|Mentioned|p58 Fig.2. |||Gawler Craton.||||||
27839|Moody Suite|64726|6|Mentioned|p83 Fig.2.|||||||||
27839|Moody Suite|64739|6|Mentioned|p264 Fig.1. |Paleoproterozoic|Paleoproterozoic|Gawler Craton.||||||
27839|Moody Suite|64828|5|Briefly described|p1064 Fig. 1|Paleoproterozoic|Paleoproterozoic|Age: ~1700Ma. Geological province: Gawler Craton. See also p1065 Fig. 2||||||04-MAR-09
27839|Moody Suite|65221|5|Briefly described|p30|Palaeoproterozoic|Palaeoproterozoic|1730-1720Ma||||||
27839|Moody Suite|65375|6|Mentioned|p13.|Paleoproterozoic|Paleoproterozoic||1708-1702 Ma.|||||
27839|Moody Suite|65376|5|Briefly described|p8 Fig.1.1, pp83-89.|Paleoproterozoic|Paleoproterozoic||||Includes Carpa Granite, Moreenia Adamellite, Chinmina Syenite, Yunta Well Leucogranite and Uranno Microgranite.|Intrudes Hutchison Group and Sleaford Complex.|Hornblende-bearing granitoids and muscovite leucogranites.|
27839|Moody Suite|65390|5|Briefly described|p19, p20, p23 Fig.3|Statherian|Statherian|Spencer Domain (southern Gawler Craton). Intermediate to felsic, syn- to post-tectonic with Kimban Orogeny. Intrudes Hutchison Group. Age of c. 1700 Ma given (Fanning, 1997).||||||
27839|Moody Suite|65485|6|Mentioned|Fig 1|Paleoproterozoic|Paleoproterozoic|||||||19-MAR-12
27839|Moody Suite|65772|6|Mentioned|p229 Fig.2, p234 Fig.8|Statherian|Statherian|1730 Ma||||||
27839|Moody Suite|65922|5|Briefly described|p13 Fig. 4, p16|Statherian|Statherian|Of Lincoln Complex. Located on the Eyre Peninsula, SA. Age of ~1780-1710 Ma given.||||||
27839|Moody Suite|66302|5|Briefly described|p4 Fig.3, p26, p34, p65|Statherian|Statherian|Spencer Domain, Gawler Craton. Ages are from SHRIMP U-Pb zircon analysis done by Fanning et al. (2007).|1720 +/- 9 Ma to 1701 +/- 12 Ma ||Includes the Moreenia Adamellite, Chinmina Monzonite and Carrapee Granite||Medium to coarse-grained, pink monzogranite, monzonite, hornblende granite, muscovite granite and leucogranite.|
27839|Moody Suite|66522|6|Mentioned|p28.|Proterozoic|Proterozoic|Gawler Craton. Likely source of zircons of this age found in Kooringa Member.|c.1730 Ma.|||||
27839|Moody Suite|67323|5|Briefly described|Eastern Australia Time-Space Plot; p33|||Gawler Craton. Syn-tectonic with the waning stages (~1725-1690 Ma) of the Kimban Orogeny.|~1715 Ma.|||||
27839|Moody Suite|67536|5|Briefly described|Map Legend|Statherian|Statherian|Gawler Craton.|1702 +/- 10 - 1692 +/- 10 Ma||||Granite to granodiorite.|
27839|Moody Suite|67980|6|Mentioned|p550|Statherian|Statherian|Schwarz (1999). Gawler Craton. Associated with Kimban Orogeny (c.1730-1690 Ma).||||||
27839|Moody Suite|68131|5|Briefly described|p2 Fig.1|Paleoproterozoic|Paleoproterozoic|Associated with the Kimban Orogeny. Mapped with Middlecamp Granite and Donington Suite as a single unit.||||||
27839|Moody Suite|68208|6|Mentioned|p32, Fig.3 |Paleoproterozoic|Paleoproterozoic|Said by Parker, Fanning & Flint (1985) to include Cooyerdoo Granite (prior to dating work).|1730 - 1700 Ma|||||
27839|Moody Suite|69004|6|Mentioned|p18|||Gawler Craton.||||||
27839|Moody Suite|69048|6|Mentioned|p2-3|Paleoproterozoic|Paleoproterozoic|Southern Eyre Peninsula.||||||
27839|Moody Suite|69649|6|Mentioned|p6 Fig.4|||||||||
27839|Moody Suite|69666|6|Mentioned|p27 Fig.3|Paleoproterozoic|Paleoproterozoic|||||||
27839|Moody Suite|70027|5|Briefly described|p56,58|Paleoproterozoic|Paleoproterozoic|Geological province: Gawler Craton. Syn-Kimban (1730-1690 Ma) Orogeny.||||Intrudes the Hutchison Group.|Monzonitic and leucogranitic rocks.|17-JUL-19
27839|Moody Suite|70382|6|Mentioned|p32|Statherian|Statherian|Geological province: Gawler Craton. Possible source for some of Quartoo Sand Member inherited zircon.|~1710 Ma||||Granite|
27839|Moody Suite|70383|6|Mentioned|p51|Statherian|Statherian|Mentioned as a possible source of zircons aged c.1732 +/- 20 Ma, extracted from the Sprigg Diamictite Member.||||||
27839|Moody Suite|70721|6|Mentioned|p63|||||||||
27839|Moody Suite|70893|5|Briefly described|p1|Statherian|Statherian|Associated with the Kimban Orogeny. |1730-1690 Ma|||||
27839|Moody Suite|71043|6|Mentioned|p107|Statherian|Statherian|Schwarz (1999).|c.1730-1700 Ma.|||||
27839|Moody Suite|71129|6|Mentioned|p40|Statherian|Statherian|Geological Province: Gawler Craton. |1710-1700 Ma|Unit of Peter Pan Supersuite.||||
27839|Moody Suite|71859|5|Briefly described|p1, p3, p16, p37|||Southern Gawler Craton.|c. 1700 Ma|||||06-APR-23
27839|Moody Suite|71862|2|Defined|p1, p3, p6-p8, p12, p15-p16, p19, p21|Statherian|Statherian|Gawler Craton. Restricted to the Tumby Bay area on the central-eastern Eyre Peninsula. The term was first used by Parker et al, 1981 to describe igneous rocks of the Lincoln Complex which were weakly deformed to unfoliated and interpreted to intrude the late stages of the Kimban Orogeny. Originally this suite included the Burkitt Granite, Carpa Granite, Wertigo Granite, Yunta Well Leucogranite, Moreenia Adamellite, Chinmina Syenite and the Uranno Microgranite. The unit was defined recently by Schwarz (1999) to include the Yunta Well Leucogranite, Moreenia Adamellite, Chinmina Syenite and the Uranno Microgranite. Some of these names have been modified in this volume. Geochemistry is broadly discussed. Originally included in the now obsolete Lincoln Complex. See also p24, p36-p40, p43-p44, p52, p62.|1720-1700 Ma|Peter Pan Supersuite|Includes the Chinmina Monzonite, Moreenia Monzogranite, Uranno Microgranite and the Yunta Well Leucogranite.|Intrudes the Hutchison Group and the Sleaford Complex.|Granite, monzogranite, monzonite and garnet- and muscovite-bearing leucogranite.|19-APR-23
27839|Moody Suite|72058|5|Briefly described|p172|||Gawler Craton. Surrounds the Middleback Ranges. Emplaced during the Kimban Orogeny.||||||
27839|Moody Suite|72459|5|Briefly described|p8, p51|Paleoproterozoic|Paleoproterozoic|Lincoln/Cleve domains of the Gawler Craton. Delineated in geophysics by ellipsoid anomalies of varying magnetic strength.|c. 1700 Ma||Includes the Carpa granite and the Chinmina syenite.|||
27839|Moody Suite|72461|6|Mentioned|p6|||Gawler Craton.|c. 1700 Ma|||||
27839|Moody Suite|72462|6|Mentioned|p3|Paleoproterozoic|Paleoproterozoic|Gawler Craton.||||||
27839|Moody Suite|72484|5|Briefly described|p2|||Associated with the transpressive, amphibolite- to granulite-facies metamorphism of the Kimban Orogeny.|1709-1701 Ma.|||||
27839|Moody Suite|73026|5|Briefly described|p6, p7, p9|Paleoproterozoic|Paleoproterozoic|Occurs on the central/western Eyre Peninsula. Emplaced during the Kimban Orogeny.|c. 1700 Ma||||Monzogranite, medium-grained; garnetiferous; granite.|
27839|Moody Suite|73027|5|Briefly described|p6, p9|Palaeoproterozoic|Palaeoproterozoic|Central/western Eyre Peninsula.|c. 1700 Ma||||Monzogranite, medium-grained, garnetiferous; granite.|
27839|Moody Suite|73030|6|Mentioned|p2149|Statherian|Statherian|Gawler Craton.||||||
27839|Moody Suite|73122|5|Briefly described|p23, 35, 42|||Eyre Peninsula.|~1710-1700 Ma.||Mikkira Granite.|Intrudes Hutchison Supergroup.|Includes syntectonic granites and pegmatites.|
27839|Moody Suite|73235|6|Mentioned|p53|Statherian|Statherian|Gawler Craton. Nuyts region.|1700 Ma|||||
27839|Moody Suite|73493|6|Mentioned|p716 Fig.3|||Gawler Craton.||||||
79272|Moola Suite|70659|5|Briefly described|p10, p42|Palaeoproterozoic|Palaeoproterozoic||1747 +/- 13 Ma (Jagodzinski and McAvaney 2016).||||Granites.|
79272|Moola Suite|70816|6|Mentioned|p3|Paleoproterozoic|Paleoproterozoic|Gawler Ranges region.||||||
79272|Moola Suite|70948|6|Mentioned|p974|Paleoproterozoic|Paleoproterozoic|Geological province: Gawler Craton.||||||
79272|Moola Suite|71037|5|Briefly described|p21 Fig.1, p22-23 Fig.2|Paleoproterozoic|Paleoproterozoic|Intruded 1745-1735 Ma, associated with Kimban Orogeny.|1745-1735 Ma.|Peter Pan Supersuite|Includes Wortham Granite, Gluepot Granite.||Syenite, granite, monzonite, diorite and gabbro, undeformed to weakly foliated.|
79272|Moola Suite|71129|4|Described|p1,40-42,177,199,225|Statherian|Statherian|Geological Province: Gawler Craton. Felsic and mafic rocks associated with early stages of Kimban Orogeny (Wade and McAvaney, 2016a). Largely restricted to northeastern and northern Eyre Peninsula. Defined by a NNW-trending magnetic high ~750m wide and ~8km long.|1745-1735 Ma|Unit of Peter Pan Supersuite.|Includes Burkitt Granite, Wortham Granite, Glue Pot Granite and Deuter Diorite.||Fine-grained weakly to moderately foliated qtz-Kfeldspar granite, weakly foliated qtz-feldspar-muscovite granite, grt-bearing leucogneiss, medium- to coarse-grained undeformed plg-Kfeldspar- qtz-hbl-bt diorite, and hbl-plagioclase-cpx amphibolite.|
79272|Moola Suite|71131|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Associated with Kimban Orogeny.|1745-1735 Ma.|Peter Pan Supersuite.|Wortham, Gluepot Granites.||Syenite, granite, monzonite, diorite and gabbro, undeformed to weakly foliated.|
79272|Moola Suite|71414|6|Mentioned|p42 Fig 1|Paleoproterozoic|Paleoproterozoic|Geological province: Gawler Craton.||||||
79272|Moola Suite|71559|6|Mentioned|p15 Fig 1|Paleoproterozoic|Paleoproterozoic|Geological province: Gawler Craton.||||||
79272|Moola Suite|71862|2|Defined|p1, p3, p6-p8, p10, p12, p19, |Statherian|Statherian|Gawler Craton. Named for the Moola Homestead 40km west-southwest of Whyalla, Eyre Peninsula. Best exposed on north-eastern Eyre Peninsula but also occurs in the eastern Gawler Craton beneath the Stuart Shelf, the Peake and Denison Inliers and Yoolerplunna Inlier and the Fowler Domain. Geochemistry is discussed broadly. Comparable geochemistry with the Pinbong Suite suggests a genetic relationship between them. Notable outcrops of unnamed granite, dolerite and amphibolite belonging to this suite are found west of Lake Gilles on the Eyre Peninsula, at Refuge Rocks and west of Iron Duke; in the northern Gawler Craton an unnamed trondhjemite/tonalite and granite gneiss are found. See also p21-p22, p25-p26, p28-p30, p41, p43-p44, p52-p58|1745-1735 Ma|Peter Pan Supersuite|Includes the Burkitt Granite, Wortham Granite, Gluepot Granite, Deuter Diorite and Wade Amphibolite.|Intrudes the Minbrie Gneiss, Hutchison Group, Moonabie Formation and is inferred to intrude the Broadview Schist.|Unfoliated to weakly foliated mica-poor granites including horblende-bearing syenite, garnet-leucogneiss as well as diorite, dolerite and amphibolite.|19-APR-23
79272|Moola Suite|72089|6|Mentioned|p3|Palaeoproterozoic|Palaeoproterozoic|Gawler Craton.||||||
79272|Moola Suite|72090|6|Mentioned|p111, p119|||Gawler Craton.||Peter Pan Supersuite||||
79272|Moola Suite|72237|6|Mentioned|p29|Paleoproterozoic|Paleoproterozoic|Geological province: Gawler Craton.||||||
79272|Moola Suite|72463|6|Mentioned|p2|Paleoproterozoic|Paleoproterozoic|||||||
79272|Moola Suite|72484|5|Briefly described|p2|||Associated with the transpressive, amphibolite- to granulite-facies metamorphism of the Kimban Orogeny.|1750-1735 Ma.|||||
79272|Moola Suite|73103|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic||~1745-1735 Ma (crystallisation).||||Granite, quartz monzonite, syenite, typically pink, medium-grained, K-feldspar-rich, mica-poor, undeformed, or with flow alignment or sporadic weak-moderate foliation; diorite, monzodiorite, monzonite, gabbro.|
79272|Moola Suite|73110|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic||~1745-1735 Ma (U-Pb).||Burkitt, Gluepot, Wortham Granites.||Granite, quartz monzonite, syenite, typically pink, medium-grained, K-feldspar-rich, mica-poor, undeformed, or with flow alignment or sporadic weak-moderate foliation; diorite, monzodiorite, monzonite, gabbro.|
79272|Moola Suite|73162|6|Mentioned|p450 Fig.2, p452 Fig.3|Paleoproterozoic|Paleoproterozoic|||||||
79272|Moola Suite|73234|6|Mentioned|p19|Statherian|Statherian|Exposed within the Six Mile Hill mapsheet.|c. 1750-1740 Ma||||Granites and felsic intrusives.|
79272|Moola Suite|73525|5|Briefly described|p19 Fig.13, p20|Statherian|Statherian|Gawler Craton, eastern.|1745-1725 Ma||Burkitt Granite, Wortham Granite, Deuter Granite, Gluepot Granite|||
24617|Moolawatana Suite|22631|6|Mentioned|table1, p176|Calymmian|Calymmian|||||||
24617|Moolawatana Suite|23478|5|Briefly described|p27|Calymmian|Calymmian|Age: ~1556 Ma.||||||
24617|Moolawatana Suite|42624|2|Defined|p23|Mesoproterozoic||Consists of Yerila, Wattleowie, Terrapinna, Prospect Hill and White Well Granites.||||||11-SEP-07
24617|Moolawatana Suite|42885|6|Mentioned|p29|||||||||
24617|Moolawatana Suite|43053|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Anorogenic granitoids.||||||26-MAY-05
24617|Moolawatana Suite|43258|5|Briefly described|Map Legend||Mesoproterozoic|||||||
24617|Moolawatana Suite|43298|5|Briefly described|Map Legend||Mesoproterozoic|||||||
24617|Moolawatana Suite|50605|5|Briefly described|p1.4, 10.2, Table 1.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Gawler Craton and Curnamona Province. Age: 1560Ma.||||||11-SEP-07
24617|Moolawatana Suite|60953|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Age: 1560-1551Ma. Anorogenic granitoids.||||||
24617|Moolawatana Suite|60959|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|||||||07-NOV-08
24617|Moolawatana Suite|61108|5|Briefly described|map legend|Mesoproterozoic|Mesoproterozoic|Anorogenic granite to adamellite. Age: 1560-1551 Ma.||||||
24617|Moolawatana Suite|63489|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Included with undifferentiated felsic intrusives. Geological Province: Mount Babbage Inlier. Age: ~1560Ma.||||||10-SEP-07
24617|Moolawatana Suite|65376|6|Mentioned|p9 Fig.1.2. |Mesoproterozoic|Mesoproterozoic|||||||
24617|Moolawatana Suite|65925|5|Briefly described|Appendix 2.||||||||Felsic intrusive rocks.|
24617|Moolawatana Suite|66302|6|Mentioned|p50, p52|Calymmian|Calymmian|Moolawatana Domain, Curnamona Province.|||Includes the Terrapinna, Wattleowie, Camel Pad, Old Camp and Yerila Granites.|||
24617|Moolawatana Suite|66518|6|Mentioned|p19 Fig.4.|Mesoproterozoic|Mesoproterozoic|Curnamona Province.|c.1560 Ma.|||||
24617|Moolawatana Suite|67536|5|Briefly described|Map Legend|Calymmian|Calymmian|Curnamona Province.|1557 +/- 6 Ma - 1556 +/- 10 Ma. ||||Granite and adamellite: 1557 +/- 6 Ma to 1556 +/- 10 Ma.|
24617|Moolawatana Suite|67581|6|Mentioned|p45|||Curnamona Province.||||||
24617|Moolawatana Suite|67653|6|Mentioned|p4|||Geological province: Curnamona Province. ||||||
24617|Moolawatana Suite|68068|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Curnamona Province.|||Includes Box Bore, Yerila, Wattleowie, Terrapinna, Prospect Hill, White Well, Con Bore and Golden Pole Granites.|||
24617|Moolawatana Suite|68126|6|Mentioned|p6|||Mount Painter Inlier, Curnamona Province.|||||Felsic intrusives.|
24617|Moolawatana Suite|68131|5|Briefly described|p2 Fig.1|Mesoproterozoic|Mesoproterozoic|Mapped with Bimbowrie and Hiltaba Suites as a single unit.|||||Granitic rocks and felsic porphyry.|
24617|Moolawatana Suite|68205|6|Mentioned|p85|||Geological province: Curnamona Province.|1555-1560 Ma||Incldues Terrapinna Granite and Yerila Granite.|||
24617|Moolawatana Suite|68713|5|Briefly described|p19, p22|Calymmian|Calymmian||ca. 1555 Ma|||Intrudes the Radium Creek Group.|Granites.|
24617|Moolawatana Suite|68715|6|Mentioned|p32 Fig.6||||||||Granitoids.|07-APR-17
24617|Moolawatana Suite|69019|5|Briefly described|p14, p23-30, p145, p163.|Calymmian|Calymmian|Curnamona Province. Of Sheard et al. (1992), Sheard (2009). Mts. Babbage and Painter Inliers. 6 other units do not outcrop in this map area. Hosts REE.|c.1555 Ma.||Includes Wattleowie, Terrapinna and Yerila Granites.|Intrudes Radium Creek Group.|Granites.|
24617|Moolawatana Suite|69023|5|Briefly described|p23, p34, p37-53, p75, p77, p158|Mesoproterozoic|Mesoproterozoic|See also p162, p189. Defined Sheard et al. (1992). Mount Babbage and Mount Painter Inliers. These granitoids are highly enriched in REE; some are quite radioactive and thus unsuitable for interior building stone. Geochemistry detailed.|~1565-1555 Ma U-Pb zircon (Neumann et al., 2009).||Includes Box Bore, Yerila, Wattleowie, Terrapinna, Prospect Hill, White Well, Golden Pole and Con Bore Granites.|Is intruded by Mudnawatana Tonalite.||
24617|Moolawatana Suite|69650|5|Briefly described|p62|Calymmian|Calymmian|Suggested to come from the same magma source as Coulthard Suite and Pepegoona Porphyry.|~1560 Ma.||Includes Terrapinna and Wattleowie Granites.|||
24617|Moolawatana Suite|69654|6|Mentioned|p3|||Curnamona Province.||||||
24617|Moolawatana Suite|70383|5|Briefly described|p44|Mesoproterozoic|Mesoproterozoic|Mount Painter Inlier.|Between c.1580 Ma and 1550 Ma.|||Intrudes Radium Creek Group.|Granites and granodiorites.|
24617|Moolawatana Suite|70384|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|There are two un-named units; one is mapped separately; the other is dated (1560 +/- 8 Ma) but not shown on the map as its known surface area is not fully determined.|||Old Camp, Camel Pad, Yerila, Wattleowie, Terrapinna, Prospect Hill, White Well, Con Bore, Golden Pole Granites; Hodgkinson Granodiorite.||Granite, quartz monzonite, granodiorite.|
24617|Moolawatana Suite|72454|6|Mentioned|p2 Fig.2|Mesoproterozoic|Mesoproterozoic|Part of the Mount Painter Inlier. Shown only on p2 Fig.2.|||||Felsic intrusive origin.|
24617|Moolawatana Suite|72456|6|Mentioned|Solid Geology Interpretation|||||||||
24617|Moolawatana Suite|72459|4|Described|p58, p63, p66-67, p70,|Mesoproterozoic|Mesoproterozoic|Mt Painter/Babbge inliers. Granites of this suite are defined by Sheard (1997). This suite outcrops in the north eastern part of Mt Painter Inlier and forms much of the Mt Babbage Inlier. In radiometric images exhibits red to reddish pink colours. Originally consisted of five phases: the Yerila Granite, Wattleowie granite, Terrapinna Granite, Prospect Hill Granite and the White Well Granite. Subdivided in this report into three so called ""sub groups"" 2a- Yerila granite, 2b-Terrapinna/Wattleowie type and 2c- Box Bore granite type. See also p73, p82-85, p94-98.|||Includes Yerila Granite, Wattleowie granite, Terrapinna Granite, White Well Granite and the Box Bore granite.|||
24617|Moolawatana Suite|72461|6|Mentioned|p6||||1556 +/- 4 Ma; 1557 +/- 4 Ma|||||
24617|Moolawatana Suite|73251|6|Mentioned|p35-37|Calymmian|Calymmian|Curnamona Province, Mount Painter and Mount Babbage inliers. Includes uraniferous crystalline rock.|c. 1560 Ma|||||
24617|Moolawatana Suite|75063|6|Mentioned|p93|Mesoproterozoic|Mesoproterozoic|Curnamona Province.|1560-1550 Ma (Sheard et al., 1992).||||Felsic igneous rocks.|
72425|Mooleugore Formation|62592|6|Mentioned|p14. |||Olary Domain, Curnamona Province.||||||
72425|Mooleugore Formation|62993|6|Mentioned|p37|Paleoproterozoic|Paleoproterozoic|Olary Domain.||Wiperaminga Subgroup||||15-DEC-21
72425|Mooleugore Formation|63102|4|Described|p14-16,18, p37|||Geological province: Olary Domain, Curnamona Province. Formerly known as Mooleugore Schist (Conor 2000a). Equivalent to 'Middle Schist' by Esso (Cotton, 1980). Base of unit defined by Esso to be above a volcanic  unit. Reference localities (see p18): i) 3 km WNW of Bimbowrie Homestead; ii) Near Mooleugore Hill; iii) Northwestern Telechie Valley (Mount Howden); iv) Eastern and southeastern Telechie Valley; and v) South of Alconie Hill.  Similar stratigraphic position to Tommie Wattie Formation.||Unit of Wiperaminga Subgroup.||Equivalent to Thackaringa Group, Thorndale Composite Gneiss, Clevedale Migmatite. Underlies the Ethiudna Subgroup.||22-OCT-19
72425|Mooleugore Formation|64944|5|Briefly described|p28 Fig. 1, p29 Tb. 1|Paleoproterozoic|Paleoproterozoic|Of Wiperaminga Subgroup (Curnamona Group). Geological province: Olary Domain. Psammitic schist with clean epidotic cross-bedded quartzite.||||||07-FEB-11
72425|Mooleugore Formation|66302|4|Described|p36 Fig.9, p37|Statherian|Statherian|Olary Domain, Curnamona Province. |ca. 1718 Ma|Wiperaminga Subgroup||Overlies the George Mine Formation.|Quartz-biotite metasedimentary rocks.|
72425|Mooleugore Formation|70657|4|Described|p14-15, p18, p23-24, p26, p29|Statherian|Statherian|Curnamona Province; Olary Domain. Formerly the Mooleugore Schist. Five reference localities described. Crops out along the SE flank of the Telechie Valley. Lateral relationship with other Formations in the Subgroup unknown. Age inferred from Tb.1. No equivalent in Broken Hill Domain.|1720 - 1715 +/- 3 Ma (~1718).|Wiperaminga Subgroup||Underlies Peryhumuck Formation (Ethiudna Subgroup).|Dark grey, fine-grained quartz-biotite psammopelitic metasediments with interlayered clean, locally epidotic, cross-bedded quartzites which locally grade into quartz albitite.|
68091|Mooleulooloo Formation|60485|6|Mentioned|p26|Statherian|Statherian|Marker unit.  See also Mooleulooloo psammopelite.||||||
68091|Mooleulooloo Formation|61736|5|Briefly described|p664, p666 Fig. 3|Paleoproterozoic|Paleoproterozoic|Of Mount Howden Subgroup (Strathearn Group) - upper part. Age: 1651+/-7Ma. Geological province: Olary Domain. Includes cream coloured, albitic, fine-grained psammites.||||||
68091|Mooleulooloo Formation|62535|4|Described|p664, p666-668, p670-672, p674|Paleoproterozoic|Paleoproterozoic|Olary Domain. A distinctive marker horizon in regional gravity surveys. Zircon age from tuffaceous source rocks.|1651 +/- 7 Ma (maximum depositional age).|Mount Howden Subgroup.||Correlated with Bijerkerno Metasediments.|Interlayered, locally tuffaceous, albitic psammites and pelites (mica schists) with siliceous concretions.|
68091|Mooleulooloo Formation|62592|5|Briefly described|p16 Fig.2.2, p76 .|||Olary Domain, Curnamona Province. Called Mooleulooloo psammopelite in Fig.2.2. Occurs in a synclinal open, upright, F3 fold.|<1651 +/- 7 Ma.|Unit in Mount Howden Subgroup.||||
68091|Mooleulooloo Formation|62993|6|Mentioned|p37|Paleoproterozoic|Paleoproterozoic|Olary Domain.|1651 +/- 7 Ma|Mount Howden Subgroup||Overlies Alconie Formation, overlain by Dayana Formation, correlated with Bijerkerno Metasediments||15-DEC-21
68091|Mooleulooloo Formation|63102|4|Described|p14,35-38|||Geological province: Olary Domain, Curnamona Province. Formerly known as Mooleulooloo Psammopelite (Conor 2000a). A distinct marker horizon on regional gravity imagery in the large polyphase synform in the vicinity of Yarramba Station, i.e. Yarramba Synform. Forms a buried ridge at the Tertiary unconformity (C. Skidmore, M. Randell and C. Giles - pers comm. 2003). U-Pb zircon age of 1648+\-3 Ma from a sample near the core of Mount Howden Syncline (Page et al. 2000).|1648 +/- 3 Ma (U-Pb)|Unit of Mount Howden Subgroup.||Equivalent to Bijerkerno Metasediments.|Thinly interlayered albitic psammites and brown mica schist. Psammites are commonly cross-bedded.|22-OCT-19
68091|Mooleulooloo Formation|63186|5|Briefly described|p67|Paleoproterozoic|Paleoproterozoic|Of the Strathearn Group (Willyama Supergroup). Geological Province: Olary Domain, Curnamona Province.||||||07-NOV-08
68091|Mooleulooloo Formation|63866|5|Briefly described|p41|||Olary Domain, Curnamona Province. Age is a U-Pb SHRIMP date and is the only constraint on the depositional age of the Willyama Supergroup in the Olary Domain.||Strathearn Group||||
68091|Mooleulooloo Formation|64741|5|Briefly described|p301 Fig. 4|Paleoproterozoic|Paleoproterozoic|Of Strathearn Group. Age: <1651+/-7Ma. Geological province: Olary Domain.||||||07-FEB-11
68091|Mooleulooloo Formation|64742|6|Mentioned|p321 Fig.3, P323. |||||Unit in Mount Howden Subgroup.|||Psammite, psammopelite.|
68091|Mooleulooloo Formation|64944|4|Described|p26, p28 Fig. 1|Paleoproterozoic|Paleoproterozoic|Of Strathearn Gp. Tuffaceous part is a chronstratigraphic marker in Olary Domain, interpreted as equiv. of Bijerkerno Metasediments inBroken Hill Domain. Dating also indicates a temporal similarity with Mount Isa Group (Qld.) Age: <1651+/-7Ma. Albitic psa||||||07-FEB-11
68091|Mooleulooloo Formation|66302|4|Described|p36 Fig.9, p38, p39|Statherian|Statherian|Olary Domain, Curnamona Province.|1651 +/- 7 Ma (Page, 2011)|Mount Howden Subgroup||Overlies the Alconie Formation, overlain by the Dayana Formation.|Thinly interlayered albitic sandstone and mica schist.|
68091|Mooleulooloo Formation|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Olary Domain.|1651 +/- 7 Ma (maximum depositional age).|Strathearn Group.||||
68091|Mooleulooloo Formation|70340|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic||U-Pb age 1648+/-6 Ma|Probably of Mount Howden Subgroup.|||Psammite, feldspathic, locally tuffaceous.|
68091|Mooleulooloo Formation|70405|4|Described|p9 table 1, p32, p43 Table 3|Paleoproterozoic|Paleoproterozoic||1640 Ma - 1655 Ma|Mount Howden Subgroup||Underlies Dayana Formation,Correlates with Bijerkerno Metasediments|Dominated by flaggy, fine to medium grained metasandstone with ripple marks and small scale crossbedding, interbedded with metasiltstone.|
68091|Mooleulooloo Formation|70657|4|Described|p13 Fig.6, p14-15, p24, p43, p45|Statherian|Statherian|Curnamona Province, Olary Domain. Previously the Mooleulooloo Psammopelite (Conor, 2000). Resistant: forms a buried ridge at the Tertiary unconformity, and crops out as the Mooleulooloo Hills. Appears as Mooleuloloo Formation in Tb.1.|1648 +/- 6 Ma (Page et al., in prep.).|Mount Howden Subgroup||Underlies Dayana Formation. Gradationally overlies Alconie Formation. Equivalent to Bijerkerno Metasediments (Paragon Group).|Thinly interlayered albitic psammites and brown mica schists, locally tuffaceous.|
68091|Mooleulooloo Formation|70658|6|Mentioned|p15|Paleoproterozoic|Paleoproterozoic|Olary Domain, Curnamona Province.|<1651 +/- 7 Ma.|Strathearn Group.||||
68091|Mooleulooloo Formation|72461|6|Mentioned|p6||||1648 +/- 6 Ma|||||
29897|Moonamby Dyke Suite|24474|5|Briefly described|p37 Fig. 2|||Geological Province: Gawler Craton.||||||
29897|Moonamby Dyke Suite|43052|5|Briefly described|p117|||Variation on Moonamby dyke-suite||||||
29897|Moonamby Dyke Suite|60484|5|Briefly described|p35|||Intrudes the Gawler Range Volcanics.  Geological Province: Gawler Craton.||||||
29897|Moonamby Dyke Suite|65376|6|Mentioned|p129.|||||||Intrudes Gawler Range Volcanics.||
29897|Moonamby Dyke Suite|67909|5|Briefly described|p125, 127, 129-130, 132-134, 136|Mesoproterozoic|Mesoproterozoic|Giles (1977). Dykes are up to 100m wide, crop out for 10-20km, and trend NW to NNE. Contains well-preserved quartz-phenocryst-hosted melt inclusions (experiments detailed).||||Cuts lower Gawler Range Volcanics.|Includes several quartz-feldpsar phyric rhyolite dykes.|
29897|Moonamby Dyke Suite|69649|5|Briefly described|p25-26|||Giles (1977). Up to 100m wide and 18km long; trending NE. Occurs only along the W margin of Lake Everard Volcanic Complex. Resembles, and may be related to intrusion of, the Hiltaba Suite. Weathers to form characteristic tors.||||Intrudes the Glyde Hill Volcanic Complex.|A series of red, highly porphyritic rhyolite and rhyodacite dykes; all have chilled margins; several contain plugs of granite.|26-FEB-15
29897|Moonamby Dyke Suite|72090|6|Mentioned|p12|||Gawler Craton.|||||Rhyolite to dacite dykes.|
36779|Moonaree Dacite Member|24346|4|Described|p103, p105|||New member of Yardea Dacite.  Formerly mapped as 'black dacite' of Yardea Dacite.||||||
36779|Moonaree Dacite Member|50127|6|Mentioned|p50|||Of the Yardea Dacite||||||
36779|Moonaree Dacite Member|70659|6|Mentioned|p6 fig 2|Mesoproterozoic|Mesoproterozoic|||Yardea Dacite||||
36779|Moonaree Dacite Member|70816|5|Briefly described|p4-5|||Gawler Ranges region.||Unit of Yardea Dacite||Underlain by Pondanna Dacite Member.|Quartz-bearing facies, includes granitic and lithic clasts.|
36779|Moonaree Dacite Member|71317|4|Described|p1, p20, p58, p85-p86, p96|Mesoproterozoic|Mesoproterozoic|Age is CA-TIMS magmatic crystallisation age. Referred to as the Moonaree Dacite on p58. Originally mapped as the Yardea Dacite before being seperated out by Allen et al., 2003. The contact with the Pondanna Dacite Member does not outcrop. Estimated thickness of at least 250m. See also p98-p99, p103-p106, p108-p114, p136, p147, p165-p166, p169-p170, p176, p193.|1587.2 +/- 0.5 Ma (Jagodzinski et al., 2016)|Yardea Dacite||Overlies the Pondanna Dacite Member and locally the Yaroo volcaniclastics.|Black, sparsely porphyritic quenched flow base, red-brown, porphyritic flow center with spherulitic to granophyric groundmass and prominent columnar jointing.|
36779|Moonaree Dacite Member|71559|4|Described|p16, p19-20, p22, p26|Mesoproterozoic|Mesoproterozoic|Geological province: Gawler Craton.||Unit of Yardea Dacite.|||Dacite, massive, red, commonly colmnar jointed; porphyritic with phenocrysts of plagioclase, pyroxene and local quartz in a fine- to medium- grained spherulitic to granophyric groundmass.|19-JUN-19
36779|Moonaree Dacite Member|71560|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Type locality near Yardea station indicated on map.||Yardea Dacite.|||Dacite, massive, red, commonly columnar-jointed; porphyritic with phenocrysts of plagioclase, pyroxene and local quartz in a fine-to medium-grained spherulitic to granophyric groundmass.|
36779|Moonaree Dacite Member|72065|4|Described|p105-110,112-116,119|Calymmian|Calymmian|Geological province: Gawler Craton. Also referred to as Moonaree Dacite in text. Dimensions: >160km E-W, 100km N-S, ~250m thick, ~3500km3. Lavas type: Peraluminous, ferroan to marginal magnesian. Emplaced in >1My from around 1588 Ma (Jagodzinski et al., 2016). Consists of red and brown facies (displays feldspar and pyroxene alteration) with subordinate basal black (no or lacking alternation of feldspars and pyroxenes) and vesicular quartz-bearing facies. See major- and trace-element composition plots on p108 Fig 5. Contains 'GRV-type' crystal clusters: pyroxene and Fe-Ti oxides+\-apatite+\-zircon+\-plagioclase. Crystal formation likely formed from the least evolved of the Upper GRV parental melt (likely hot, dry, and relatively reduced, as pyroxenes predominate over biotite). Interpreted that crystals formed within the magmatic system, and required a subsequent event or rejuvenation (magma recharge: increased temperature or melt volatile content for example) to free the crystal clusters prior to, and during extrusive unit emplacement.||Unit of Yardea Dacite.||Uppermost unit of the Gawler Range Volcanics.||
36779|Moonaree Dacite Member|72089|5|Briefly described|p2|||Gawler Craton.  Rapidly erupted.||Yardea Dacite|||Dacitic lava.|
36779|Moonaree Dacite Member|72090|6|Mentioned|p12|||Gawler Craton.|1586.5 +/- 0.5 Ma|Yardea Dacite, Gawler Range Volcanics, Upper||||
36779|Moonaree Dacite Member|72462|6|Mentioned|p8|||||Yardea Dacite, Gawler Range Volcanics||||
36779|Moonaree Dacite Member|73110|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic||||||Dacite, massive, red, commonly columnar jointed; porphyritic with phenocrysts of plagioclase, pyroxene.|
34325|Moondrah Gneiss|22629|5|Briefly described|fig2 fig147,156|Statherian|Statherian|Proposed name. In Ooldea region. Age: 1700Ma||||||
34325|Moondrah Gneiss|22851|5|Briefly described|13|Paleoproterozoic|Paleoproterozoic|Name Proposed||||||07-NOV-08
34325|Moondrah Gneiss|23481|5|Briefly described|p19 Fig 1|||Geological Province: Gawler Craton.||||||
34325|Moondrah Gneiss|23805|5|Briefly described|p4 Fig. 1|Paleoproterozoic|Paleoproterozoic|Geological Province: Gawler Craton.||||||07-NOV-08
34325|Moondrah Gneiss|24505|5|Briefly described|p5 Fig. 1|||Geological Province: Gawler Craton.||||||15-SEP-05
34325|Moondrah Gneiss|24526|6|Mentioned|p100|Paleoproterozoic||Age: 1650+/-8Ma (SHRIMP U-Pb zircon, Fanning 1997).||||||07-NOV-08
34325|Moondrah Gneiss|60484|5|Briefly described|p33 Fig. 1|||Geological Province: Gawler Craton.||||||
34325|Moondrah Gneiss|60515|6|Mentioned|p116 Fig.1 |||||||||
34325|Moondrah Gneiss|61522|5|Briefly described|p5 Fig.1|||Geological Province: Gawler Craton.||||||
34325|Moondrah Gneiss|61659|5|Briefly described|p30 Fig.1, p41.|Paleoproterozoic|Paleoproterozoic|Nawa Domain, Gawler Craton. Experienced very high temperature metamorphism c.1650 Ma, given the new term Ooldean Orogeny in this article.||||||
34325|Moondrah Gneiss|61864|6|Mentioned|p16 fig 3|||||||||
34325|Moondrah Gneiss|62978|5|Briefly described|p163, p170|Paleoproterozoic|Paleoproterozoic|In the Nawa Domain.  Highly magnetised belt of rocks. Age: 1653+/-8Ma (SHRIMP). Geological Province: Gawler Craton.||||||07-FEB-11
34325|Moondrah Gneiss|63866|5|Briefly described|p6, p9-p11, p22, p32|||Wilgena and Nawa Domains, Gawler Craton. Has a relatively high magnetic intensity. Metamorphic date is provided from Fanning et al., 2007.|1659 +/- 6 Ma (U-Pb zircon, metamorphism)||||Variably mylonitised, iron-rich, magnetite-bearing migmatitic gneisses.|
34325|Moondrah Gneiss|64130|5|Briefly described|p1378 Fig.1, p1387 |Paleoproterozoic|Paleoproterozoic|Metamorphosed at 1693 +/- 9 Ma (Kimban orogeny) and 1649 +/- 7 Ma (Ooldean event) .|~1740 Ma||||Granulite facies metapelites.|
34325|Moondrah Gneiss|64722|6|Mentioned|Fig. 5 p.13|Paleoproterozoic|Paleoproterozoic|Of South Australian Craton.||||||
34325|Moondrah Gneiss|64739|6|Mentioned|p264 Fig.1. |Paleoproterozoic|Paleoproterozoic|Gawler Craton.||||||
34325|Moondrah Gneiss|65376|5|Briefly described|p8 Fig.1.1, pp154-159. |Paleoproterozoic|Paleoproterozoic|Nawa Domain, Gawler Craton. High-temperature metamorphism occurred about 1659 +/- 6 Ma.|Max.depositional age of c.1740 Ma.||||Iron-rich metasediments, probable iron-formations; locally upper amphibolite to lower granulite-facies BIF, garnet quartzite, porphyroblastic garnet gneiss and peridotitic ultramafic rock.|
34325|Moondrah Gneiss|65390|6|Mentioned|p13, p22 Fig. 3|Statherian||Mis-spelt Moondra in Fig.3. Nawa Domain of Gawler Craton. Age of >1650 Ma given. Magnetite-rich metasediments, thought to represent aluminous, magnesium-rich meta-pelites.||||||
34325|Moondrah Gneiss|65922|6|Mentioned|p13 Fig. 4|||Gawler Craton.||||||
34325|Moondrah Gneiss|66302|5|Briefly described|p4 Fig.3, p19, p32, p53, p76 Fig.20|||Nawa Domain, Gawler Craton. Highly magnetised. Preserves evidence of UHT metamorphic conditions (950 C, 9.5 Kbar). Metamorphic SHRIMP U-Pb age of 1659 +/- 6 Ma.|||||Variably mylonitised, iron-rich, magnetite-bearing, migmatitic gneisses.|
34325|Moondrah Gneiss|67323|5|Briefly described|Eastern Australia Time-Space Plot, p32|||Nawa Basin, Gawler Craton.|~1760-1740 Ma: protolith deposition.|||||
34325|Moondrah Gneiss|67536|5|Briefly described|Map Legend||Siderian|Gawler Craton.|Ooldea inheritance 2426 +/- 6 Ma.||||Granulite-grade iron-rich aluminous metasediments; precursor of unknown age.|
34325|Moondrah Gneiss|67980|5|Briefly described|p554-555, p559-560, p563-564, p566|||SHRIMP U-Pb zircon age for timing of high-grade metamorphism in Karari Shear Zone. The same sample yields a 40Ar/39Ar biotite plateau age of 1507 +/- 5 Ma. Payne et al. (2008) reported a monazite age of 1688 +/- 9 Ma from this unit, interpreted to reflect timing of granulite-facies metamorphism. Age issues discussed in text.|1692 +/- 6 Ma (Fraser et al., 2012).||||Pink and blue-grey banded gneiss, with K-feldspar augen wrapped by dark, magnetite-bearing ribbons.|
34325|Moondrah Gneiss|69004|6|Mentioned|p18|||Gawler Craton.|||||Paragneisses.|
34325|Moondrah Gneiss|69203|5|Briefly described|p10|||Nawa Domain.|||||Includes ultra-high-temperature quartz-sapphirine-bearing granulites.|
34325|Moondrah Gneiss|69648|4|Described|p12 Fig.6, p13-15, p16, p34, map legend|Mesoproterozoic|Palaeoproterozoic|Nawa Subdomain. Identified in drill core from several holes. Magnetite-rich metasediments which Daly et al. (1998) considered to represent aluminous, magnesium-rich metapelites. LA ICPMS U-Pb dating (detrital zircons in metasedimentary rocks, from drillholes, within Nawa Subdomain) suggested a maximum depositional age of around 1740 Ma, with predominance between 1740-1840 Ma (Payne et al., 2006).|max depositional age ~1740 Ma||||High-grade metasediments which include magnetite-rich zones of high magnetic intensity; granulite facies gneisses, includes hypersthene + sillimanite + quartz, and ultra-high temperature assemblage sapphirine + quartz (Purvis in Miller et al., 1982)|17-FEB-15
34325|Moondrah Gneiss|69649|6|Mentioned|p6 Fig.4||||||||Includes paragneisses.|23-FEB-15
34325|Moondrah Gneiss|71341|5|Briefly described|p181|Palaeoproterozoic|Palaeoproterozoic|Nawa Domain, Gawler Craton. A metamorphic age of ca. 1713-1688 Ma is derived from monazite in this unit (Payne et al, 2008) and ca. 1692 from metamorphic zircon (Fraser et al., 2012).|||||Iron-rich, pelitic gneiss.|
34325|Moondrah Gneiss|71859|5|Briefly described|p3|Paleoproterozoic|Paleoproterozoic|||||||
34325|Moondrah Gneiss|71862|6|Mentioned|p3|||||||||
34325|Moondrah Gneiss|72459|6|Mentioned|p22|||Nawa subdomain. Records the timing of an ultra-high temperature metamorphic event (>950C, 950Kbar) in zircons dated by Teasdale (1997) between roughly 1690 Ma and 1653 Ma.||||||
34325|Moondrah Gneiss|72462|6|Mentioned|p3|Paleoproterozoic|Paleoproterozoic|Gawler Craton.||||||
34325|Moondrah Gneiss|72478|6|Mentioned|p6|||Nawa Domain. Affected by the c. 1660 Ma Ooldean Event. Iron-rich basement unit. Underlies Officer Basin. Also misspelt twice as Moondra Gneiss p6, from the Ooldea DDH2 drillhole.|||||Includes ultra-high temperature quartz?sapphirine-bearing granulites and iron-rich rocks.|25-MAR-21
34325|Moondrah Gneiss|73111|5|Briefly described|Map legend.|||Is shown in the Solid Geology Interpretation map below the main MAURICE map.||||||
39174|Moonta Porphyry Member|24475|2|Defined|p53|Paleoproterozoic|Paleoproterozoic|Of Weetulta Formation. Formerly Moonta Porphyry.||||||07-NOV-08
39174|Moonta Porphyry Member|60958|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Weetulta Formation.  Massive, fine-grained to porphyritic rhyolite, rhyodacite to dacite. A Type. Age: 1760 +/- 7Ma. Geological Province: Gawler Craton.||||||07-NOV-08
39174|Moonta Porphyry Member|61121|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Weetulta Formation. Massive, fine-grained to porphyritic rhyolite, rhyodacite to dacite.  Extrusive to intrusive. A-type.Glomeroporphyritic texture; foliated. Age: ~1800Ma.Geological Province: Gawler Craton.||||||07-NOV-08
39174|Moonta Porphyry Member|65375|4|Described|p19, p22, p26. |Paleoproterozoic|Paleoproterozoic|Hosts the Cu-Au deposits in Moonta area. Geochemically resembles A-type granites. Foliated and recrystallised.|1760 +/- 7 Ma to 1737 +/- 5 Ma. |Unit in Weetulta Formation.||Interdigitated with biotite schist of Doora Member. Locally overlain by Winulta Formation in erosional channels.|Porphyritic rhyolite to rhyodacite; massive to layered; intrusive or extrusive; uniform, LREE enriched with an average SiO2 of 71.35%|
39174|Moonta Porphyry Member|65376|4|Described|pp101-105, p109. |||Type section is in DDH East Moonta 2. Interpreted as series of ignimbrites or subaerial flows with adjacent epiclastic sediments and/or waterlain tuffs. Primary host for Moonta Cu-Au lodes.|1753 +/- 8 Ma to 1748 +/- 15 Ma.|Unit in Weetulta Formation.||Intercalated with Doora Member at Kadina.|Rhyolite to dacite.|
39174|Moonta Porphyry Member|66302|5|Briefly described|p29, p33|||Olympic Domain, Gawler Craton. ||Weetulta Formation||Intercalated with the Doora Member.|Felsic porphyritic rocks.|
39174|Moonta Porphyry Member|67181|5|Briefly described|p629|Statherian|Statherian|Gawler Craton. ca 1750 Ma from Fanning et al. 2007|ca 1750 Ma|Unit in Weetulta Formation.||||
39174|Moonta Porphyry Member|69748|6|Mentioned|p179-183, 187-193, 196-199|Paleoproterozoic|Paleoproterozoic|Moonta-Wallaroo region, Olympic IOGC Province. The ""Member"" component of the name is, more often than not, omitted. REY fractionation trends graphed. LA-CP-MS data for REE, Pb, Th, U and other elements tabulated.||Weetulta Formation.|||Felsic volcanic rocks: rhyodacitic. Highly altered.|
39174|Moonta Porphyry Member|70383|6|Mentioned|p51|Statherian|Statherian|Mentioned as a possible source of zircons aged c.1732 +/- 20 Ma, extracted from the Sprigg Diamictite Member.||||||
39174|Moonta Porphyry Member|73092|6|Mentioned|p27, p32|Statherian|Statherian|Age is of magmatic crystallisation. Dated sample is fine grained granite from drillhole CUR D5 (78.5-78.9 m); sample tentatively assigned to this unit based on similar ages.|c. 1750 Ma, 1737 +/- 28 Ma||||Includes foliated medium- to fine-grained granodiorite.|
27294|Mooracoochie Volcanics|13497|4|Described|p49, p55, p83, p90, p114|Early Cambrian|Early Cambrian|Warburton Basin.||||Overlain by the Kalladeina Formation.|Rhyodacites, basalts and pyroclastic rocks.|
27294|Mooracoochie Volcanics|22527|6|Mentioned|p 3|||||||||
27294|Mooracoochie Volcanics|23154|5|Briefly described|Map Legend|Cambrian|Cambrian|Geological Province - Warburton Basin.||||||
27294|Mooracoochie Volcanics|23155|4|Described|p8|Early Cambrian|Early Cambrian|An agglomerate within the Mooracoochie Volcanics contains hyolithid and trilobite fossils of Cambrian age.||||||
27294|Mooracoochie Volcanics|23854|5|Briefly described|p863|Early Cambrian|Early Cambrian|||||||
27294|Mooracoochie Volcanics|24482|5|Briefly described|p44|||Geological Province: Warburton Basin.||||||
27294|Mooracoochie Volcanics|38661|2|Defined|p6|Early Cambrian|Early Cambrian|||||||
27294|Mooracoochie Volcanics|40642|4|Described|p167|||Mention p162.||||||04-APR-07
27294|Mooracoochie Volcanics|40830|6|Mentioned|p8|||||||||
27294|Mooracoochie Volcanics|41288|6|Mentioned|Fig.7|||||||||
27294|Mooracoochie Volcanics|42064|5|Briefly described|p167|||||||||
27294|Mooracoochie Volcanics|42246|6|Mentioned|p17|||||||||
27294|Mooracoochie Volcanics|42274|6|Mentioned|p458|||||||||
27294|Mooracoochie Volcanics|42357|5|Briefly described|p4|||||||||
27294|Mooracoochie Volcanics|42746|4|Described|p3, Fig.2 p5|||||||||
27294|Mooracoochie Volcanics|43560|6|Mentioned|Table 7,p231|||Age: >520 Ma||||||
27294|Mooracoochie Volcanics|44133|5|Briefly described|p4 Fig. 7.2, 14, 31|Early Cambrian|Early Cambrian|Geological Province: Eastern Warburton Basin. Overlies and intertongues with Pando Formation. Has been divided into two informal units.||||||04-APR-07
27294|Mooracoochie Volcanics|63056|5|Briefly described|p81 Fig. 2|Early Cambrian|Early Cambrian|Includes Taloola Ignimbrite Member. Thickness: 990m. Geol. Province: Warburton Basin. Volcaniclastics - tuff, ignimbrite; sand and silt; carbonate brecciated, containing Cambrian fossil fragments; porphyritic trachyte, shattered/pentrated by dacitic lava.||||||
27294|Mooracoochie Volcanics|63978|5|Briefly described|p5|Early Cambrian|Early Cambrian|Overlies and interfingers with Pando Formation. Geological province: Warburton Basin. Acid and basic lavas, tuffs and volcaniclastic sedimentary rocks interbedded with minor shallow marine sedimentary rocks.||||||07-FEB-11
27294|Mooracoochie Volcanics|65337|5|Briefly described|p95.|||Warburton Basin. Possible correlative with Kalkarindji Volcanic Group.||||Is unconformably overlain by Kalladeina Formation.||
27294|Mooracoochie Volcanics|65489|4|Described|p28-29, p32 Fig.11, p74, p96, p119-121|Early Cambrian|Early Cambrian|Gatehouse (1983). Oldest rocks in Eastern Warburton Basin. Includes all the major volcanics in the Basin. Over 120m thick. Hosts Sturt 6 and 7 oil, and gas in Lycosa 1 and Moolallie 1.|517 +/- 9 Ma (U-Pb zircon).||Includes Taloola Ignimbrite Member.|Correlates with Truro and Mount Wright Volcanics, and the Cymbric Vale Formation.|Porphyritic trachyte, dacitic lava, volcaniclastics: tuff, ignimbrite; sand and silt; brecciated fossiliferous carbonate.|
27294|Mooracoochie Volcanics|65686|5|Briefly described|p420|||Warburton Basin, beneath fossiliferous section.|517 +/- 9 Ma.|||||07-MAY-12
27294|Mooracoochie Volcanics|65925|5|Briefly described|Appendix 2.||||||||Tuff, lapilli tuff, trachyte, rhyolite and crystal tuff, conglomerate and agglomerate.|
27294|Mooracoochie Volcanics|67105|5|Briefly described|p650|Early Cambrian|Early Cambrian|Warburton Basin. Aeromagnetic lineaments appear to link the Koonenberry Belt under cover ~200km to the NW of the Mount Wright Arc. Mis-spelt as Moorachoochie Volcanics.||||Correlated with the Mount Wright Volcanics.|Calc-alkaline volcanics; subsurface.|
27294|Mooracoochie Volcanics|67402|4|Described|p239, p260, p261|Early Cambrian|DESC|Warburton Basin. Unsuitable reservoir for the storage of carbon dioxide. 990m thick. ||||Unconformably overlain by the Diamond Bog Dolomite.|Volcaniclastics, tuff, ignimbrite, porphyritic trachyte, sand and silt.|
27294|Mooracoochie Volcanics|67536|5|Briefly described|Map Legend|Stage 5|Stage 2|Warburton Basin.|ca. 517 +/- 9 Ma||||Volcaniclastics, porphyritic trachyte, dacite.|
27294|Mooracoochie Volcanics|68731|5|Briefly described|p115, p168, p170 Fig 3.83, p171, p217|Series 3|Terreneuvian|Warburton Basin. ~ 990 m thick.|517 +/- 9 Ma (PIRSA 2007)|||Overlain by the Diamond Bog Dolomite.|Comprise acid and basaltic lavas, tuffs and volcaniclastic sedimentary rocks interbedded with minor shallow marine sedimentary rocks.|
27294|Mooracoochie Volcanics|68822|6|Mentioned|p329|Stage 5||Warburton Basin.|> 508 Ma|||||
27294|Mooracoochie Volcanics|69019|6|Mentioned|p80 Fig.17, p145.|||Described in comparison with Ooloo Hill Formation basalts.||||||
27294|Mooracoochie Volcanics|69023|5|Briefly described|p82, p149|Early Cambrian|Early Cambrian|Dominant source of clasts for Merrimelia Formation conglomerate. Rb-Sr ages for this unit had been reset by magmatism and deformation in the eastern Warburton Basin during the late Devonian.||||Is overlain by Merrimelia Formation.||
27294|Mooracoochie Volcanics|69445|5|Briefly described|p30:17|Middle Cambrian||Gatehouse (1983). Warburton Basin.||||Is overlain unconformably by Kalladeina Formation. Possible correlate of Kalkarindji Suite.||12-JUL-16
27294|Mooracoochie Volcanics|69449|5|Briefly described|p34:1; 34:2 Fig.34.2|Cambrian||Eastern Warburton Basin.||||Is overlain unconformably by Kalladeina Formation.|Acid-intermediate volcanic rocks, tuff and agglomerate.|12-JUL-16
27294|Mooracoochie Volcanics|69673|6|Mentioned|p149 fig 120|||||||||
27294|Mooracoochie Volcanics|69728|6|Mentioned|p285|Cambrian|Cambrian|Warburton Basin.|||Jena Basalt.||Bimodal volcanics.|
27294|Mooracoochie Volcanics|69982|3|Fully described|p15, p10,p13-15, p17-19, p22, p29, p42,|Early Cambrian|Early Cambrian|See also p44-45, p51-52, p54-55, p148, p162-164, p220, p223-224, Appendix 1. Gatehouse (1983). Type section in Gidgealpa 3 well. At least 989m thick; not yet fully penetrated. Deposition or emplacement during initial rifting of the Warburton Basin. Includes all the major volcanics in the Basin. Hosts 24% of the oil shows in the Basin and 9% of the gas shows: hosts the Sturt 6 gas reservoir. Reservoir attributes described. Brief thin section descriptions. Composite logs shown. Bedding dip angles in wells listed. Details of wells with hydrocarbon shows.|517 +/- 9 Ma (U-Pb: Armstrong, 1995).||Includes Taloola Ignimbrite Member.|Is overlain by Jena Basalt or unconformably by Toolachee Formation.|Includes trachyte, rhyolite, rhyodacite, dacite and latite; minor basalt; local ignimbrites and associated volcaniclastic rocks including syn-eruptive hyaloclastites and carbonates, epiclastic conglomerates and sandstones; possibly local andesite.|12-NOV-15
27294|Mooracoochie Volcanics|70033|5|Briefly described|p4, p48|Early Cambrian|Early Cambrian|The basal Warburton Basin consists of an early Cambrian intermediate to silicic volcanic and volcaniclastic succession (Gatehouse 1986; Radke 2009).|517 +/- 9 Ma, unpubl. U-Pb age, Armstrong 1995|||||
27294|Mooracoochie Volcanics|70749|5|Briefly described|p43-45|Cambrian|Cambrian|Warburton Basin. Extends into undercover Thomson Orogen. No enclosing sediments to assess terrestrial or marine environment. Another age of 510.0 +/- 2.8 Ma (Draper, 2006) is given.|517 +/- 9 Ma.||||Altered, fine-grained, crystal- and lithic-poor welded rhyolitic ignimbrite.|
27294|Mooracoochie Volcanics|71283|5|Briefly described|p471, p472 Fig.2|Cambrian|Cambrian|Gatehouse (1983, 1986). Warburton Basin. Defined to include all the major volcanic units in the Basin.|||||Trachytes, rhyolite and possibly andesite.|
27294|Mooracoochie Volcanics|71342|6|Mentioned|Ch10 tbl 10.1, Ch10 p20|Cambrian|Cambrian|Warburton Basin.||||||
27294|Mooracoochie Volcanics|71965|6|Mentioned|p894|||Geological province: Thomson Orogen.||||||
27294|Mooracoochie Volcanics|71966|5|Briefly described|p989,991,999|Cambrian|Cambrian|Geological province: Thomson Orogen. Of Warburton Basin. Similar age to magmatism of the Mount Wright Arc (NSW) and Stavely Arc (VIC); Gatehouse (1986) and Scheiber and Veevers (2000) suggested a continuation of this arc magmatism into the Warburton Area as the Gidealpa Arc, however Purdy et al. (2013) has contested the tectonic affinities of Warburton volcanics (e.g. Moorachoochie Volcanics) to the Mount Wright and Stavely arcs. Sample intersected in drillhole DIO Adria Downs 1 is thought to be linked to the Mooracoochie Volcanics; weighted mean 206Pb/238U age of 509.7+\-3.8M a, interpreted as eruptive age. Interpreted A-type geochemistry of this sample indicate an extensional non-arc environment. Hf and O isotopic analysis indicate derivation from an evolved supracrustal source; similar to the Mooracoochie Volcanics.||||||
27294|Mooracoochie Volcanics|72951|6|Mentioned|p1012|Cambrian|Cambrian|Warburton Basin. May be a northward extension of the Mount Wright Arc. Described as lower Cambrian.||||||
27294|Mooracoochie Volcanics|73244|6|Mentioned|p86|Cambrian|Cambrian|Warburton Basin.|||||Volcaniclastic.|
27294|Mooracoochie Volcanics|73479|5|Briefly described|p155, p156 Fig.2|Cambrian|Cambrian|Marks the base of the Warburton Basin.||||Unconformably underlies Diamond Bog Dolomite|Volcanoclastic.|
23808|Moorillana Member|24397|5|Briefly described|p242|||Of Benbow (1993).  Authors recommend name be avoided pending further clarification of unit.  Of Hampton Sandstone.  Geological Province: Eucla Basin.||||||
23808|Moorillana Member|42816|5|Briefly described|p23|||of Hampton Sandstone||||||
29933|Moorilyanna Formation|23282|6|Mentioned|p68|||||||||
29933|Moorilyanna Formation|43052|5|Briefly described|Table 2.1 p27|||Moorilyanna Graben. ?Neoproterozoic - Cambrian.||||||
29933|Moorilyanna Formation|43053|5|Briefly described|Map Legend|Cambrian|Cambrian|Conglomerate, arkose, shale, siltstone.||||||01-APR-14
29933|Moorilyanna Formation|43258|5|Briefly described|Map Legend||Cambrian|||||||
29933|Moorilyanna Formation|43298|6|Mentioned|Map Legend||Cambrian|||||||
29933|Moorilyanna Formation|44133|5|Briefly described|p38-39|Middle Paleozoic|Early Paleozoic|Previously known as Moorilyanna Conglomerate.||||||07-NOV-08
29933|Moorilyanna Formation|67536|6|Mentioned|Map Legend|||Moorilyanna Graben.|||||Pebble conglomerate, arkose, quartzite, minor siltstone and dolomite.|01-APR-14
29933|Moorilyanna Formation|70839|5|Briefly described|p345|||Occurs in Moorilyanna Graben. Thick, poorly exposed succession of immature siliciclastic rocks in inferred faulted contact with crystalline basement of eastern Musgrave region. Possible interpretations include early Palaeozoic syn-tectonic deposits related to Petermann Orogeny (Gravestock et al., 1995), or latest Mesoproterozoic equivalents of Bloods Range Formation and Dixon Range beds (Morton and Drexel, 1997). Contains congloemrates with abundant fresh basement-derived clasts.||||||
26042|Moornaba Sand|23342|5|Briefly described|28 Fig.1|Holocene|Pleistocene|||||||
26042|Moornaba Sand|23719|4|Described|p29|Holocene|Holocene|See also page 30 table 9. Overlying unit Saint Kilda Formation. Geological Province: Gawler Craton. Max. thickness: 15 m.||||||
26042|Moornaba Sand|30756|2|Defined|p2|Recent|Recent|||||||
26042|Moornaba Sand|30922|6|Mentioned|Map legend|Holocene|Holocene|||||||
26042|Moornaba Sand|35772|4|Described|Table 1|||||||||
26042|Moornaba Sand|39349|6|Mentioned|Map legend|Holocene|Holocene|||||||
26042|Moornaba Sand|40448|5|Briefly described|p43|||||||||
26042|Moornaba Sand|41499|6|Mentioned|p70|||||||||
26042|Moornaba Sand|41619|6|Mentioned|Map legend|Holocene||||||||
26042|Moornaba Sand|42475|5|Briefly described|p24|||||||||
26042|Moornaba Sand|42716|5|Briefly described|Map legend|Holocene||||||||
26042|Moornaba Sand|42721|5|Briefly described|map legend|Holocene||||||||
26042|Moornaba Sand|42722|5|Briefly described|map legend|Holocene|Holocene|Vegetated seif dunes and sand spreads; pale yellowish brown, orange-brown and brownich quartz sands, with soft carbonates in places.||||||07-APR-05
26042|Moornaba Sand|42738|5|Briefly described|map legend|Quaternary||||||||
26042|Moornaba Sand|43049|5|Briefly described|p28|||||||||
26042|Moornaba Sand|43071|5|Briefly described|p17,Table 3|||||||||
26042|Moornaba Sand|43094|5|Briefly described|p40|||||||||
26042|Moornaba Sand|44864|5|Briefly described|Map Legend||Holocene|||||||
26042|Moornaba Sand|61155|5|Briefly described|p17|Holocene|Late Pliocene|Age: <2Ma. Geological Province: Eucla Basin.||||||
26042|Moornaba Sand|62893|4|Described|Map Legend, p24|Holocene|Holocene|Forms spreads of modem dunes and veneers over the Pleistocene longitudinal dunes from which it is derived within the Corrobinnie Depression. Thick native vegetation stabilizes the dunes, although massive stripping for agriculture has allowed reworking and partial remobilisation.||||Equivalent to Semaphore Sand.|White, pale grey and orange quartz sand.|
26042|Moornaba Sand|65922|5|Briefly described|p25 Tb. 4, p27-28|Holocene|Holocene|Pale creamish white and locally pale orange, fine to medium-grained, well-sorted quartz sand. Interfingers with Wiabuna Formation. Forms extensive northwest to west-trending dunes, the cores of which may be Wiabuna Formation. ||||||
26042|Moornaba Sand|69649|5|Briefly described|p33|||2-10m thick. Sief-dune pattern blankets and mimics the calcreted Pleistocene inland dunes of the Great Victoria Desert. |||||Orange to pale yellow quartz sands.|
26042|Moornaba Sand|70337|5|Briefly described|Map legend.|Holocene|Holocene||||||Sand, aeolian, off-white and pale yellow, quartz-rich with carbonate pipes.|
26042|Moornaba Sand|70893|6|Mentioned|p3 fig 1b|Holocene|Holocene|||||||
26042|Moornaba Sand|71317|5|Briefly described|p1, p143, p150-p151, p153|Holocene|Pleistocene |Constitutes the main part of the Ilkina Dunefield.||||Overlies the Garford Formation and the Wiabuna Formation.|Pale, yellowish-orange, medium- to coarse-grained, moderately to well sorted sand dominated by subangular to subrounded quartz grains and minor agnular to subrounded calcrete grains.|
26042|Moornaba Sand|71559|5|Briefly described|p19|Holocene|Holocene|Geological province: Gawler Craton.|||||Sand, aeolian, off-white and pale yellow, quartz-rich with carbonate pipes.|
26042|Moornaba Sand|71560|5|Briefly described|Map legend.|Holocene|Holocene||||||Sand, aeolian, off-white and pale yellow, quartz-rich with carbonate pipes.|
26042|Moornaba Sand|73103|5|Briefly described|Map legend.|Holocene|Holocene||||||Sand, aeolian, off-white and pale yellow, quartz-rich with carbonate pipes.|
26042|Moornaba Sand|73110|5|Briefly described|Map legend.|Holocene|Holocene||||||Sand, aeolian, off-white and pale yellow, quartz-rich with carbonate pipes.|
26042|Moornaba Sand|73302|6|Mentioned|p34|Holocene|Holocene|||||||
26314|Moralana Supergroup|23309|5|Briefly described|p38-40, 45, 46.|Early Cambrian|Early Cambrian|Was "Glenelg River beds".  Ages:  572+/-9Ma, 558+/-6Ma, 556+/-6Ma, 553+/-9Ma, 551+/-6Ma, but noted as " Probably geologically meaningless mixed ages between detrital mica and new growth in the Delamerian".||||||04-MAY-10
26314|Moralana Supergroup|24551|5|Briefly described|p74|||||||||
26314|Moralana Supergroup|24586|5|Briefly described|p51 Fig. 1|Early Cambrian|Early Cambrian|Includes the Hawker Group. Geological Province: Adelaide Geosyncline.||||||05-JUL-06
26314|Moralana Supergroup|38004|2|Defined|p82|Precambrian|Precambrian|||||||
26314|Moralana Supergroup|38703|6|Mentioned|p131|||||||||
26314|Moralana Supergroup|38704|6|Mentioned|p133|||||||||
26314|Moralana Supergroup|39344|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
26314|Moralana Supergroup|41401|5|Briefly described|p32|||||||||
26314|Moralana Supergroup|42028|6|Mentioned|p137|||||||||
26314|Moralana Supergroup|42215|6|Mentioned|Fig.2 P448|||||||||
26314|Moralana Supergroup|42239|6|Mentioned|Fig.2 P151|||||||||
26314|Moralana Supergroup|42882|5|Briefly described|Table 1 P3|||||||||
26314|Moralana Supergroup|43052|5|Briefly described|p172|||||||||
26314|Moralana Supergroup|43595|5|Briefly described|p545||Cambrian|||||||
26314|Moralana Supergroup|43845|5|Briefly described|Fig2 p42||Early Cambrian|||||||12-JUL-16
26314|Moralana Supergroup|50154|2|Defined|p47, p52, p249 App.5|Cambrian|Cambrian|Geological Province: Delamerian Fold Belt.||||||15-SEP-04
26314|Moralana Supergroup|50155|5|Briefly described|Map Legend|||||||||
26314|Moralana Supergroup|50156|5|Briefly described|Map Legend|||||||||
26314|Moralana Supergroup|50157|5|Briefly described|Map Legend|||||||||
26314|Moralana Supergroup|50158|5|Briefly described|Map Legend|||||||||
26314|Moralana Supergroup|50159|5|Briefly described|Map Legend|||||||||
26314|Moralana Supergroup|50160|5|Briefly described|Map Legend|||||||||
26314|Moralana Supergroup|50161|5|Briefly described|Map Legend|||||||||
26314|Moralana Supergroup|50162|5|Briefly described|Map Legend|||||||||
26314|Moralana Supergroup|50163|5|Briefly described|Map Legend|||||||||
26314|Moralana Supergroup|50164|5|Briefly described|Map Legend|||||||||
26314|Moralana Supergroup|60451|5|Briefly described|p21 Fig. 7, 106|Late Cambrian|Middle Cambrian|Geological Province: Adelaide Geosyncline.||||||
26314|Moralana Supergroup|60959|5|Briefly described|Map Legend|Middle Cambrian|Early Cambrian|||||||
26314|Moralana Supergroup|62592|5|Briefly described|p50 Table 5.1.|Early Cambrian|Early Cambrian|Adelaide Geosyncline.|||Includes Hawker and Lake Frome Groups, Billy Creek Formation and Wirrealpa Limestone.|Disconformably overlies Heysen Supergroup.||
26314|Moralana Supergroup|62742|5|Briefly described|p698|Cambrian|Cambrian|Contains a quartz-rich sandstone.||||||21-OCT-08
26314|Moralana Supergroup|64314|5|Briefly described|p495 Fig. 2a|Cambrian|Cambrian|||||||
26314|Moralana Supergroup|64801|6|Mentioned|p110 Fig.2, p111|Middle Cambrian|Early Cambrian|Arrowie Basin.||||Overlies Heysen Supergroup.||
26314|Moralana Supergroup|65375|5|Briefly described|p33.|Cambrian|Cambrian||||Includes all Cambrian units on Yorke Peninsula, from Winulta Formation to Yuruga Formation.|||
26314|Moralana Supergroup|65376|5|Briefly described|p9 Fig.1.2. |Paleozoic|Paleozoic||||||Largely marine sediments and metasediments including limestone and dolomite; minor volcanics.|
26314|Moralana Supergroup|65379|5|Briefly described|p643|||Includes Normanville and Hawker Groups. A major stratigraphic subdivision of the Adelaide Geosyncline.||||||07-MAR-12
26314|Moralana Supergroup|65716|5|Briefly described|p4|Cambrian|Ediacaran|Sedimentary rocks. Enclose Truro Volcanics. Thought to be Early Cambrian. Younger than 500-600 Ma (detrital zircons).||||||
26314|Moralana Supergroup|65925|5|Briefly described|Appendix 2.||||||||Red, white feldspathic sandstone; minor pyritic shale; siltstone; fossiliferous oolitic stromatolitic limestone with minor sandstone and siltstone.|
26314|Moralana Supergroup|66002|5|Briefly described|p4 Tb.1|Cambrian|Cambrian|Includes Glenelg River Metamorphic Complex, Nangeela Formation and Truro Volcanics. Defined in Preiss 1982. See also VandenBerg et al 2000.||||||
26314|Moralana Supergroup|68030|6|Mentioned|p236|||Flinders Ranges.||||||
26314|Moralana Supergroup|68131|5|Briefly described|p2 Fig.1|Cambrian|Cambrian|Largely marine.|||||Sediments and metasediments including limestone and dolomite, minor volcanics.|
26314|Moralana Supergroup|69019|5|Briefly described|p66-70.|Cambrian|Cambrian|Of Preiss (1982) for all Cambrian sediments of the Adelaide Geosyncline: Stansbury and Arrowie Basins.|||Includes Hawker and Lake Frome Groups.|||
26314|Moralana Supergroup|70407|5|Briefly described|p102 Fig 1, p103 Fig 2|Early Cambrian|Early Cambrian||||Includes Hawker Group.|||
26314|Moralana Supergroup|70718|5|Briefly described|p37|Middle Cambrian|Neoproterozoic|||||||
26314|Moralana Supergroup|71593|4|Described|p20-p21, p198|Cambrian|Cambrian||||Includes the Normanville and Kanmantoo Groups.|||
26314|Moralana Supergroup|72445|6|Mentioned|App.7 p6 Fig.3.|Cambrian|Cambrian|Shown only on the geological map covering the Stavely Project area (from Geology of Victoria 2003: 21).||||||
26314|Moralana Supergroup|73177|6|Mentioned|p1114||||||Billy Creek Formation.|||
26314|Moralana Supergroup|73222|6|Mentioned|p6|Cambrian|Early Cambrian|Adelaide Rift Complex.|||Hawker Group|||
26314|Moralana Supergroup|74367|5|Briefly described|p4, p6, p22|Cambrian|Cambrian||||Normanville Group, Kanmantoo Group, Lake Frome Group||Sandstones, carbonates and shales.|
27201|Mordinyabee Rhyodacite|30984|2|Defined|p12|Proterozoic|Proterozoic|||||||
27201|Mordinyabee Rhyodacite|41974|6|Mentioned|Fig.1 P408|||||||||
80751|Moreenia Monzogranite|71862|4|Described|p7, p15, p17-p18, p24|Statherian|Statherian|Originally the Moreenia Adamellite of Schwarz (1999). Outcrops in the Moody Tank area and near the Cummins-Buckleboo railway between Cockaleechie and Moody Railway siding. Contains abundant xenoliths of monzogranite phases and metasedimentary xenoliths. Foliation is highly variable. See also p36-p37, p39-p41, p43, p62.|1720 +/- 9 Ma (magmatic, Fanning et al, 2007)|Moody Suite||Intrudes (inferred) the Hutchison Group.|Medium-grained porphyritic monzogranite.|28-FEB-19
74613|Morgan Subgroup|64237|5|Briefly described|p18, p19|Middle Miocene|Early Miocene|Demoted from Morgan Group of Lukasik and James (1998) when their revision of Murray group up to Murray Supergroup was not accepted. This was formerly the Morgan Limestone of the original stratigraphic scheme of Ludbrook (1961).||||||
29837|Morialpa Migmatite|22884|2|Defined|p40 Fig. 1, p39||Paleoproterozoic|New name, lowest known unit of the Willyama Supergroup. Overlain by Tommie Wattie Formation. Max. thickness: 3000m. Migmatite and composite gneiss.||||||26-MAR-09
29837|Morialpa Migmatite|63102|5|Briefly described|p19|||Geological province: Olary Domain, Curnamona Province. Nomenclature of Laing (1996b), to replace informal name od Composite Gneiss Suite of Clarke et al., 1986. Represents parts of the Wiperaminga Subgroup, which have experienced a high degree of partial melting as a result of Olarian Orogeny. Occurs as large bodies of elongated zones interlayered with less metamorphically altered rocks.||Unit of Wiperaminga Subgroup.|||Quartzofeldspathic composite gneiss and migmatite.|
29837|Morialpa Migmatite|66302|6|Mentioned|p39|||||||||
29837|Morialpa Migmatite|70657|5|Briefly described|p25|||Laing (1996). Suggested in this study that this name be used rather than the Composite Gneiss Suite of Clarke et al. (1986). Represents parts of the Wiperaminga Subgroup that have experienced a high degree of partial melting. Result of Olarian Orogeny. Occur interlayered with less altered rocks, and as aureoles surrounding some ~1590 Ma Ninneie Supersuite granites.||Wiperaminga Subgroup.||||
80327|Morney beds|70823|5|Briefly described|p40, p44|||Cooper Basin. Deposited in floodplain or meandering fluvial environments.| APT4.2|||Unconformably overlies the Tinchoo Formation.||31-JAN-18
80327|Morney beds|70824|5|Briefly described|p7|Norian|Norian|Cooper Basin. Deposited as floodplain or meandering fluvial deposits.||||Unconformably overlies the Tinchoo Formation.||
30072|Morum Formation|12796|5|Briefly described|p462, p456 Fig. 2|Santonian|Coniacian|Of Sherbrook Group. Replaces Belfast Mudstone in the Port Campbell Embayment area specifically. Interfingers with and overlain by Mount Salt Formation. Geological Province: Otway Basin/Gambier Embayment.||||||
22396|Mount Aloysius Complex|44109|3|Fully described|p26-39, p136|Mesoproterozoic|Mesoproterozoic|Felsic granulite; derived from igenous protoliths; mafic granulite layers and lenses; metasedimentary rocks, including quartzite, metapelite and calc-silicate granulite, orthogneiss, syenite.||||||
22396|Mount Aloysius Complex|61339|5|Briefly described|Map legend|||||||||
22396|Mount Aloysius Complex|69153|6|Mentioned|GA_geochron.csv|||25 samples described. 23 samples refer to: Sun, S.S. Gray, C.M. Sheraton, J.W. 1995. Zircon U-Pb chronology and neodymium isotope study of tectono-thermal and crustal forming events in the Tomkinson Ranges, western Musgrave Block, Central Australia.|||||Felsic gneiss, felsic and intermediate and mafic intrusives, metasediment; granite, gabbronorite dyke, quartz monzodiorite, quartz monzodiorite and pelite.|
22396|Mount Aloysius Complex|70634|5|Briefly described|GA_geochron.csv|Paleoproterozoic|Paleoproterozoic|Sample Descriptions: BT granite augen gneiss (rapakivi), GNT-PL-QZ-KFS gneiss, porphyritic BT-HBL quartz monzonite (rapakivi), OPX-BT-CPX quartz monzodiorite|1901 Ma - 2118 Ma (Sm-Nd)|||||
22396|Mount Aloysius Complex|71592|5|Briefly described|Appendix A.|||Musgrave Province. Metamorphosed at 1223 +/- 7 Ma (U-Pb zircon SHRIMP).|1305+/-8 Ma (crystallisation: U-Pb zircon SHRIMP)||||Gneiss.|
78582|Mount Burr Volcanic Group|68990|6|Mentioned|p459|||(Sprigg 1952; Sheard 1990, 1995). Spelt as Mt Burr Volcanic Group in the text. Also written as Mt Burr volcanic group on p453. Sediments over lying ash deposits in Lake Leake are >50, 000 years BP (older than radiocarbon dating).||||||19-DEC-13
27500|Mount Curtis Tillite|22510|5|Briefly described|p40|||A 'through-going' diamictite unit of the Yerelina Subgroup (together with the Pepuarta Tillite).  Age: Marinoan.  Overlies the Fortress Hill Formation in the northern Flinders Ranges.||||||13-OCT-04
27500|Mount Curtis Tillite|22772|5|Briefly described|Table13.1|Neoproterozoic III|Neoproterozoic III|Written: 'Mt Curtis Tillite'||||||
27500|Mount Curtis Tillite|22857|5|Briefly described|Tb. 13.1 (insert p70-71)|Marinoan|Marinoan|Of the Yerelina Subgroup (Umberatana Group). Mount is Mt. in text of figure.||||||
27500|Mount Curtis Tillite|23394|5|Briefly described|Map legend|Proterozoic|Proterozoic|||||||
27500|Mount Curtis Tillite|23411|6|Mentioned|Map Legend|||||||||
27500|Mount Curtis Tillite|23804|6|Mentioned|p17|||||||||
27500|Mount Curtis Tillite|23818|5|Briefly described|p64 Fig.22, p72|Adelaidean|Adelaidean|Mount is spelt Mt. in text. Of the Yerelina Sub-Group. Max. thickness: ~300 ft. Underlying unit: Trezona and Amberoona Formations.||||||
27500|Mount Curtis Tillite|24175|4|Described|p13|Neoproterozoic III|Neoproterozoic|Of Yerelina Subgroup.  Laminated siltstone with dropstones, including numerous quartzite clasts.  Overlies Fortress Hill Formation.  Max. thickness: 200m.||||||
27500|Mount Curtis Tillite|24176|4|Described|p13, p24 Tb. 1|Adelaidean|Adelaidean|Of the Yerelina Sub-Group.  Boulder beds.  Underlies Balparana Sandstone; overlies Fortress Hill Formation; intertongues with Elatina Formation.  Max. thickness: 90m. Age is Marinoan.  Geological Province: Mount Painter Province.||||||
27500|Mount Curtis Tillite|24321|5|Briefly described|Map legend|Adelaidean|Adelaidean|Parent: Yerelina Subgroup||||||
27500|Mount Curtis Tillite|30176|6|Mentioned|Map legend|Adelaidean|Adelaidean|Marinoan||||||
27500|Mount Curtis Tillite|30177|2|Defined|p132, p85, p86-87|||Age said to be Adelaidean (Marinoan). Type section 0.3 mile northwest of Mount Saturday, lat. 30degres07'27"S  long. 13915'54"E to lat. 30degrees 07'31"S long. 139 degrees 15'50" E. Thickness 300 feet (90 metres). Previously designated an unnamed member of the Yerelina "Formation".||Yerelina Sub-Group.||Overlies conformably Fortress Hill Formation. Transitionally succeeded by Balparana Sandstone.|Massive grey-green slightly dolomitic greywacke tillite.|26-NOV-22
27500|Mount Curtis Tillite|30261|6|Mentioned|Table 1|||Marinoan age||||||
27500|Mount Curtis Tillite|30801|6|Mentioned|p5|||Marinoan Table P5-6||||||
27500|Mount Curtis Tillite|30807|6|Mentioned|p102|||Suggested map symbol||||||
27500|Mount Curtis Tillite|32724|6|Mentioned|Fig.1|||Correlation. Marinoan||||||
27500|Mount Curtis Tillite|33474|6|Mentioned|Fig.2|||||||||
27500|Mount Curtis Tillite|34535|5|Briefly described|p72|||Yerelina Sub-Group||||||
27500|Mount Curtis Tillite|34812|6|Mentioned|Table 8|||||||||
27500|Mount Curtis Tillite|35255|6|Mentioned|Fig.7|||||||||
27500|Mount Curtis Tillite|36137|5|Briefly described|p16|||Palaeomagnetism discussed.||||||
27500|Mount Curtis Tillite|36253|6|Mentioned|Fig.3-2|||||||||
27500|Mount Curtis Tillite|36733|6|Mentioned|Table 5|||||||||
27500|Mount Curtis Tillite|37461|6|Mentioned|p342|||||||||
27500|Mount Curtis Tillite|37932|5|Briefly described|p546|||See also p544.||||||14-JUN-22
27500|Mount Curtis Tillite|38157|6|Mentioned|Table IV|||||||||
27500|Mount Curtis Tillite|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Marinoan||||||
27500|Mount Curtis Tillite|40910|6|Mentioned|p12|||||||||
27500|Mount Curtis Tillite|40911|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
27500|Mount Curtis Tillite|41236|5|Briefly described|p65|||||||||
27500|Mount Curtis Tillite|41405|3|Fully described|p197|||Mention Fig.48. The type section was specified about 1 km north of Mount Saturday (from lat. 30degrees06'53"S, long. 139degrees16'27"E to lat. 30degrees07'27"S, long. 139degrees15'34"E), where the unit is about 1 070 m thick.||||||26-NOV-22
27500|Mount Curtis Tillite|42222|6|Mentioned|p18|||||||||
27500|Mount Curtis Tillite|42238|5|Briefly described|Table 1 P74|||||||||
27500|Mount Curtis Tillite|42239|6|Mentioned|p161|||||||||
27500|Mount Curtis Tillite|42542|5|Briefly described|p8|||||||||
27500|Mount Curtis Tillite|42813|6|Mentioned|p21|||||||||
27500|Mount Curtis Tillite|43052|5|Briefly described|p190,Table 6.1|||of Yerelina Subgroup||||||
27500|Mount Curtis Tillite|64797|6|Mentioned|p166 Tb.7|||||||||
27500|Mount Curtis Tillite|65379|5|Briefly described|p643, p644|Neoproterozoic|Neoproterozoic|Of Umberatana Group (Heyson Supergroup). Diamictite, massive, with dolomitic and silty matrix. N.B. Asbestos deposit host, contains Mt Fitton area asbestos occurrence.||||||07-MAR-12
27500|Mount Curtis Tillite|68241|6|Mentioned|p20 Fig.1|||Spelt as Mt. Curtis Tillite in the text.||||||
27500|Mount Curtis Tillite|69019|4|Described|p51-53.|Neoproterozoic|Neoproterozoic|Defined by Coats (in Coats and Blissett, 1971). Type section is immediately N of Mt Saturday where it is ~90 m thick. Records the Elatina glacial maxima in northern Flinders Ranges.||Unit in Yerelina Subgroup.||Conformably overlies Gumbowie Arkose and Fortress Hill Formation.|Massive grey-green diamictite with minor laminated intervals; scattered dropstones in a poorly sorted grey-green dolomitic and silty matrix; local (Moolawatana Suite granite) boulder concentrations.|
27500|Mount Curtis Tillite|70384|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Adelaide Geosyncline. About 5km S of Mount Fitton Talc Mines, includes clasts up to 3 x 8m of Terrapinna Granite. Age shown more specifically as Marinoan [Cryogenian].||Of Yerelina Subgroup.|||Massive diamictite with minor laminated intervals; scattered rounded to sub-rounded granules to pebbles (quartzite, dolomite, granite porphyry) in poorly sorted grey-green dolomitic and silty matrix. Local boulder concentrations.|23-JAN-19
27500|Mount Curtis Tillite|72456|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Marree 1:250k map sheet. |||||Diamictite, massive, with dolomitic and silty matrix.|
36781|Mount Double Ignimbrite|24346|4|Described|p103, p105|||Mount is Mt. in text.  Orginally mapped as part of the "black (Yardea) dacite" of Yardea Dacite.||||||
36781|Mount Double Ignimbrite|70659|5|Briefly described|p8|Mesoproterozoic|Mesoproterozoic|Gawler Ranges.||Upper Gawler Range Volcanics.||||
36781|Mount Double Ignimbrite|70816|6|Mentioned|p5|||Gawler Ranges region.||Unit of upper Gawler Range Volcanics.||||
36781|Mount Double Ignimbrite|71559|6|Mentioned|p17|||Geological province: Gawler Craton. A lithologically distinct and regionally extensive marker bed within upper Gawler Range Volcanics.||||Correlative to the Mount Friday Formation.||
36781|Mount Double Ignimbrite|72065|6|Mentioned|p105|Calymmian|Calymmian|Geological province: Gawler Craton.||Unit of Gawler Range Volcanics.||||
36781|Mount Double Ignimbrite|72090|6|Mentioned|p12|||Gawler Craton.||Gawler Range Volcanics, Upper||||
79616|Mount Friday Formation|71317|2|Defined|p1, p26, p54-p72, p75, p80|Mesoproterozoic|Mesoproterozoic|Name derived from Mount Friday southeast of Hiltaba Homestead. Outcrops near Mount Friday on Peltabinna are nominated as the type area for this unit (from GDA94 53 516115 mE 6436048 to 518349 mE 6433576 mN). Deposited in a continental subaerial fluvio-lacustrine setting within a volcanically active environment. Distribution, outcrop characteristics, alteration, descriptions at outcrops and in drillholes are discussed. Age derived from dating of units underlying and overlying. Intersected in MSDP05(drillhole 288771) and MSDP07 (drillhole 288773) which is proposed as a reference section. Where this unit intercalates with the Yannabie Rhyolite member is an anomalous zone of alteration and quartz-pyrite veining containing Ag, Pb, Cu, Mo, As, Bi and Sb. Up to 90m thick in MSDP07 with an average preserved thickness of 10-20m in outcrop. A stratigraphic log of the formation is provided on p69. Locally overlain by the Yardea Dacite. See also  p84-p85, p96, p104, p155-p156, p158, p171-p172, p192-p193.|1587.5-1587.2 |Gawler Range Volcanics||Disconformably overlies the Paney Rhyolite Member. Locally overlies the Eucarro Rhyolite. Disconformably overlies or is interbedded with the Yannabie Rhyolite Member.|Massive, very poorly sorted, matrix-supported, diamictic volcanic lithic breccias that grade to massive, clast-bearing volcanic mudstones that are intercalated with clast-supported volcanic conglomerates, volcanic sandstones and volcanic siltstones.|
79616|Mount Friday Formation|71559|4|Described|p17, p19-22|Mesopreoterozoic|Mesopreoterozoic|Geological province: Gawler Craton. A lithologically distinct and regionally extensive marker bed within upper Gawler Range Volcanics. Up to 90m thick in MSDP05 and MSDP07. In part silicified, hematised and or overprinted by sericite and chlorite alteration.||Unit of Upper Gawler Range Volcanics.||Deposited in contact between Yardea Dacite and, sometimes intercalated with, Eucarro Rhyolite. Outcrops of Mount Friday Fm are underlain by Paney Rhyolite.|Poorly sorted, matrix supported volcanic lithic breccias, conglomerates grading into clast-bearing volcanic mudstones. Local intercalations of better sorted, clast-supported volcanic conglomerates, volcanic sandstones and rare laminated siltstones.|29-MAY-19
79616|Mount Friday Formation|71560|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|||Upper Gawler Range Volcanics.|||Volcaniclastic breccia, conglomerate, diamictite, sandstone and siltstone.|
79616|Mount Friday Formation|72090|5|Briefly described|p47, p50, p55, p57, p59, p110|||Gawler Craton. Additional lithologies are described.|||||Epiclastic volcanic breccia, volcanogenic sedimentary deposits and pseudobreccia developed in porphyritic dacite.|
79616|Mount Friday Formation|73162|6|Mentioned|p459|||Mount is spelt Mt in text. Lateral extent limited to 3.5 km.||upper Gawler Range Volcanics|||Includes sediments up to 90 m thick.|
28796|Mount Gambier Volcanic Complex|35147|4|Described|p125|||Discussed throughout article.||||||
28796|Mount Gambier Volcanic Complex|37500|6|Mentioned|p387|||||||||
28796|Mount Gambier Volcanic Complex|40521|6|Mentioned|p313|||||||||
28796|Mount Gambier Volcanic Complex|40561|6|Mentioned|p8|||||||||
28796|Mount Gambier Volcanic Complex|42097|5|Briefly described|p46|||See also Figs. 6 and 7||||||
27205|Mount Gee Sinter|41258|2|Defined|p23|Silurian|Late Ordovician|Formerly Mount Gee Beds.||||||11-SEP-07
27205|Mount Gee Sinter|42871|5|Briefly described|p90|||actually spelt Mt Gee Sinter||||||
27205|Mount Gee Sinter|43053|5|Briefly described|Map Legend|||spelt Mt Gee Sinter||||||
27205|Mount Gee Sinter|43201|4|Described|p13|||||||||
27205|Mount Gee Sinter|43258|5|Briefly described|Map Legend|Permian|Carboniferous|Mount is Mt in text.||||||11-SEP-07
27205|Mount Gee Sinter|43298|6|Mentioned|Map Legend|Permian|Carboniferous|spelt Mt Gee Sinter.||||||
27205|Mount Gee Sinter|44133|5|Briefly described|p57|||Thickness: 200m.||||||
27205|Mount Gee Sinter|60953|5|Briefly described|Map Legend|Permian|Carboniferous|Hydrothermal deposits. Mount is Mt in text.||||||27-APR-05
27205|Mount Gee Sinter|61108|5|Briefly described|map legend|Carboniferous|Carboniferous|Spelt Mt on map legend. Hydrothermal uranium-bearign granitic, haematitic, and chloritic breccia and quartz-haematite sinter.||||||
27205|Mount Gee Sinter|61523|5|Briefly described|p8|||Quartz-hematite unit. Geological Province: Mount Painter Inlier.||||||
27205|Mount Gee Sinter|63489|5|Briefly described|Map legend|Permian||Age: ?Carboniferous to Permian. Geological Province: Mount Painter Inlier. Granitic, chloritic and haematitic uraniferous breccias and local diamictite dykes; massive to layered, vuggy quartz-haematite sinter.||||||10-SEP-07
27205|Mount Gee Sinter|64329|6|Mentioned|p18|||||||||
27205|Mount Gee Sinter|65925|5|Briefly described|Appendix 2.||||||||Quartz-haematite, rhythmically layered, vuggy.|
27205|Mount Gee Sinter|67430|5|Briefly described|p39-41, 43, 56-57|||Mount Gee - Mount Painter area, Mount Painter Inlier. See also references to Mount Gee Unit (p39-41, 56). At least 200m thick locally. Hosts low quantities of U and Cu.||||Cross-cuts Radium Ridge Breccias.|Discontinuous, locally highly vughy, zones of banded quartz and hematite (60:40 volume ratio), with layers of quartz that supports clasts of coarse specular hematite, and finely laminated quartz-hematite.|
27205|Mount Gee Sinter|70383|5|Briefly described|p43-45, p52-53|Pliocene|Valanginian|Resulted from a long-standing episodic hydrothermal system. Fills large vughs within the Radium Ridge Breccias. May be as young as Tertiary [Paleogene - Neogene].||||Crosscuts Sprigg Diamictite Member and Radium Ridge Breccias.||16-JAN-19
27205|Mount Gee Sinter|70384|5|Briefly described|Map legend.|Pliocene|Late Cretaceous|Maximum age from crosscutting relationship.|< ~264 Ma.|||Crosscuts Sprigg Diamictite Member.|Sinter, epithermal-hydrothermal, quartz-haematite, rhythmically layered, vuggy.|
35886|Mount Howden Subgroup|23347|2|Defined|p52 Fig. 2, p54|Statherian|Statherian|Supersedes "Mount Howden Formation". Of the Strathearn Group (Willyama Supergroup).  Age: 1692+/-3Ma, >/-1648+/-6Ma. Overlies Ethiudna Subgroup, and Saltbush Subgroup in places. Psammopelitic metasediments, + lesser psammite and pelite. Equiv.to Paragon Gp||||||26-FEB-13
35886|Mount Howden Subgroup|24431|5|Briefly described|p189 Fig. 1|||Of the Strathearn Group. Overlies the Saltbush Subgroup. Geological Province: Olary Domain.||||||24-FEB-10
35886|Mount Howden Subgroup|60485|5|Briefly described|p28 Fig. 2|||Of the Strathearn Group (Willyama Supergroup). Geological Province: Olary Domain. Mount may be Mt in text.||||||03-MAR-05
35886|Mount Howden Subgroup|61734|5|Briefly described|p52 Fig.2|Statherian|Statherian||1.65 Ga|Of the Strathearn Group||Overlies Saltbush Subgroup.|Dominantly pelitic.|
35886|Mount Howden Subgroup|61736|5|Briefly described|p666 Fig. 3|Paleoproterozoic|Paleoproterozoic|Of Strathearn Group. Contains Alconie, Mooleulooloo and Dayana Formations. Geological province: Olary Domain. Mount is Mt in text.||||||
35886|Mount Howden Subgroup|62373|5|Briefly described|p503 Fig.2|Paleoproterozoic|Paleoproterozoic|Of the Strathearn Group (Willyama Supergroup). Geological Province: Curnamona Province/Olary Domain.||||||07-NOV-08
35886|Mount Howden Subgroup|62514|5|Briefly described|p748 Fig. 3|Mesoproterozoic|Mesoproterozoic|Of Strathearn Group. Age: >1650Ma. Geological Province: Olary Domain/Curnamona Province||||||16-SEP-09
35886|Mount Howden Subgroup|62535|4|Described|p663, p666-668, p670-674|Paleoproterozoic|Paleoproterozoic|Olary Domain.|1651 +/- 7 Ma (maximum depositional age).||Alconie, Mooleulooloo, Dayana Formations.|Correlated with Paragon Group.|Includes tuffaceous sedimentary rocks.|
35886|Mount Howden Subgroup|62592|5|Briefly described|p14, p16 Fig.2.2.|||Olary Domain, Curnamona Province. There is a hiatus of c. 40 m.y. between deposition of Plumbago Formation and this unit.||Unit in Strathearn Group.|Includes Mooleulooloo Formation.|||
35886|Mount Howden Subgroup|62993|6|Mentioned|p37|Paleoproterozoic|Paleoproterozoic|Olary Domain.||Strathearn Group|Includes Alconie Formation, Mooleulooloo Formation, Dayana Formation|||15-DEC-21
35886|Mount Howden Subgroup|63020|5|Briefly described|p987 Fig. 8|Paleoproterozoic|Paleoproterozoic|Age: 1651+/-7Ma. Geological Province: Curnamona Province (Olary Domain).||||||07-NOV-08
35886|Mount Howden Subgroup|63102|5|Briefly described|p13-15,26-27,32-33,36-39,59|||Geological province: Olary Domain, Curnamona Province.||Unit of Strathearn Group.|Includes Dayanna, Mooleulooloo and Alconie formations.|Underlain by Plumbago Formation. Equivalent to Paragon Group and Cartwrights Creek Metasediments.||22-OCT-19
35886|Mount Howden Subgroup|63186|5|Briefly described|p67 Fig. 3|Paleoproterozoic|Paleoproterozoic|Of the Strathearn Group (Willyama Supergroup). Geological Province: Olary Domain, Curnamona Province. Mount is Mt in text.||||||24-FEB-10
35886|Mount Howden Subgroup|64741|5|Briefly described|p301 Fig. 4|Paleoproterozoic|Paleoproterozoic|Of Strathearn Group. Includes Alconie Formation. Geological province: Olary Domain.||||||07-FEB-11
35886|Mount Howden Subgroup|64742|5|Briefly described|p321 Fig.3, p323, p325, pp332-333.|||Major and trace element analyses, and Sm-Nd isotope data, are detailed.||Unit in Strathearn Group.|Includes Alconie, Mooleulooloo and Dayana Formations.|||
35886|Mount Howden Subgroup|64743|6|Mentioned|p342. |Paleoproterozoic|Paleoproterozoic|Olary Block.||||Lateral equivalent to Paragon Group, Broken Hill Block.||
35886|Mount Howden Subgroup|64744|6|Mentioned|p353 Fig.4, p356.|Statherian|Statherian|Olary Domain.||Unit in Willyama Supergroup.||Overlies Saltbush Subgroup.||
35886|Mount Howden Subgroup|64944|5|Briefly described|p28 Fig. 1, p29 Tb. 1|Paleoproterozoic|Paleoproterozoic|Of Strathearn Group. Geological province: Olary Domain.||||||07-FEB-11
35886|Mount Howden Subgroup|66302|5|Briefly described|p36 Fig.9, p39|Statherian|Statherian|Olary Domain, Curnamona Province.|1670-1640 Ma|Strathearn Group|Includes the Alconie Formation, Mooleulooloo Formation and the Dayana Formation.|||
35886|Mount Howden Subgroup|70339|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|||Willyama Supergroup.|||Psammopelite; lesser psammite and pelite.|27-JAN-16
35886|Mount Howden Subgroup|70340|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|||Probably includes Mooleulooloo Formation.|||Psammopelite; lesser psammite and pelite.|
35886|Mount Howden Subgroup|70405|6|Mentioned|p27, p30|Paleoproterozoic|Paleoproterozoic|Disconformable on the Saltbush Group||Strathearn Group|Includes Alconie Formation, Mooleulooloo Formation, Dayana Formation|Overlies Larry Macs Subgroup, Bimba Formation and Plumbago Formation, correlated to Paragon Group|Commonly characterised by abundant chiastolite porphyroblasts.|
35886|Mount Howden Subgroup|70657|5|Briefly described|p13 Fig.6, p14-15, p17, p24, p39-40|Statherian|Statherian|See also p42-43, p65. Curnamona Province, Olary Domain. Also Mt Howden Subgroup in Tb.1.||Strathearn Group|Alconie, Mooleulooloo, Dayana Formations.|Appears to correlate with parts of Paragon Group in Broken Hill Domain. Overlies Plumbago Formation, Saltbush Group.||
35886|Mount Howden Subgroup|70658|5|Briefly described|p15|Paleoproterozoic|Paleoproterozoic|Olary Domain, Curnamona Province.||Strathearn Group.|Alconie, Dayanna Formations.|||
35886|Mount Howden Subgroup|72461|6|Mentioned|p6|||||||||
35886|Mount Howden Subgroup|73429|5|Briefly described|p106 Fig.2|Statherian|Statherian|Curnamona Province, Olary Domain||Strathearn Group||Overlies Walparuta Formation||
34769|Mount Johns Conglomerate Member|22922|6|Mentioned|33 fig 2|Early Cambrian|Early Cambrian|Mount as 'Mt' in text. Of Apamurra Formation, Officer Basin.||||||
34769|Mount Johns Conglomerate Member|23282|2|Defined|p78||Early Cambrian|Age: Early Cambrian 518 - 516Ma. Introduced by Krieg (1973) and defined by Benbow (1982). It is here redefined as a member of Apamurra Formation, Officer Basin.||||||
34769|Mount Johns Conglomerate Member|24112|5|Briefly described|p254 Fig.2|Early Cambrian|Early Cambrian|Mount is spelt Mt. in text. Of the Marla Group. Geological Province: Officer Basin||||||
34769|Mount Johns Conglomerate Member|62570|5|Briefly described|p580 Figs. 2 and 3|Middle Cambrian|Middle Cambrian|Of Apamurra Formation (Marla Group). Geological Province: Officer Basin. Mount is Mt in text.||||||10-AUG-07
34769|Mount Johns Conglomerate Member|70336|5|Briefly described|Map legend|Cambrian|Cambrian|||Of Apamurra Formation.|||Poorly sorted, red-brown conglomerate; cross-bedded feldspathic sandstone.|12-JAN-16
34769|Mount Johns Conglomerate Member|72478|6|Mentioned|p8|Early Cambrian|Early Cambrian|||Base of Apamurra Formation.||||
34769|Mount Johns Conglomerate Member|73090|5|Briefly described|Appendix.|Cambrian|Cambrian||||||Conglomerate, poorly sorted, red-brown; cross-bedded feldspathic sandstone.|
23824|Mount Mantell Member|40431|2|Defined|p12|Early Cambrian|Early Cambrian|Atdabanian||||||
23824|Mount Mantell Member|42233|4|Described|p249|||See also Fig.2||||||
23824|Mount Mantell Member|69570|6|Mentioned|p421-p423|||At least 171m thick.||Wilkawillina Limestone||Disconformably overlies the Woodendinna Dolomite. Overlain by the Hideaway Well Member.||
23824|Mount Mantell Member|70833|5|Briefly described|p180,183-185,187-188,190,201,203|Terreneuvian|Terreneuvian|Of Arrowie Basin. Key sections: MORO (S of Moro Gorge, Arrowie Syncline); BALC (Balcoracana Gorge, Bunkers Range); MMT (Bunkers Range, central Flinders Ranges); WILK (Bunkers Graben); 10MS-W (Ten Mile South, SE Bunkers Graben). Originally defined on shallow platform successions in the Bunkers Graben and Range (Clarke, 1986a). Depositional environment: shallow shelf carbonate. Incised into underlying Woodendinna Dolostone.||Unit of Wilkawillina Limestone.||Laterally grades into Wirrapowie Limestone. Overlain by Hideaway Well Member. Underlain by Woodendinna Dolostone.||
23824|Mount Mantell Member|70835|6|Mentioned|p336|Cambrian|Cambrian|Arrowie Basin, Flinders Ranges.||Wilkawillina Limestone.||Is overlain by Hideaway Well Member.||
23824|Mount Mantell Member|71102|5|Briefly described|p267|Terreneuvian|Terreneuvian|Of Arrowie Basin.||||Lowermost unit of Wilkawillina Limestone. Overlain by Hideaway Well Member. Underlain by Woodendinna Dolostone.||
26054|Mount Margaret Quartzite|22889|6|Mentioned|p31|Adelaidean|Adelaidean|Parent - Emeroo Subgroup.||||||
26054|Mount Margaret Quartzite|23054|5|Briefly described|p11-2,21|||||||||
26054|Mount Margaret Quartzite|23818|5|Briefly described|p38 Fig.10|Adelaidean|Adelaidean|Mount is spelt Mt in text. Of the Burra Group.||||||18-APR-05
26054|Mount Margaret Quartzite|24506|5|Briefly described|p18 Fig. 4|Neoproterozoic|Neoproterozoic|Developed a land surface which now remains as a remnant known as the Mount Margaret Surface.  Overlain by Skillogalee Dolomite.||||||19-SEP-05
26054|Mount Margaret Quartzite|31798|4|Described|Fig. 1|||Torrensian||||||
26054|Mount Margaret Quartzite|33939|6|Mentioned|p410|||Adelaidean||||||
26054|Mount Margaret Quartzite|34535|6|Mentioned|p59|||Burra Gp.||||||
26054|Mount Margaret Quartzite|34537|6|Mentioned|Fig.10|||||||||
26054|Mount Margaret Quartzite|36733|2|Defined|p10|Adelaidean|Adelaidean|See also P12,23,40.||||||
26054|Mount Margaret Quartzite|37854|6|Mentioned|Table 1|||||||||
26054|Mount Margaret Quartzite|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Torrensian||||||
26054|Mount Margaret Quartzite|40294|6|Mentioned|Table 2|||||||||
26054|Mount Margaret Quartzite|41404|5|Briefly described|p89|||||||||
26054|Mount Margaret Quartzite|42274|5|Briefly described|p450|||||||||
26054|Mount Margaret Quartzite|43052|5|Briefly described|p177,Table 6.2|||of Emeroo Subgroup||||||
26054|Mount Margaret Quartzite|44289|5|Briefly described|Map Legend||Neoproterozoic|||||||
26054|Mount Margaret Quartzite|62453|6|Mentioned|p14|Torrensian|Torrensian|||||||
26054|Mount Margaret Quartzite|64796|5|Briefly described|p191 Fig.9, p192|Neoproterozoic|Neoproterozoic|Lobate deltaic sand body.||||Is overlain by Skillogalee Dolomite.||
25287|Mount McDonnell Formation|22581|4|Described|Fig.2,p37|||Of the Kangaroo Island Group. Thickness: 300 m. Overlain by Stokes Bay Sandstone||||||02-JUL-08
25287|Mount McDonnell Formation|22643|5|Briefly described|fig3p187, fig6|Early Cambrian|Early Cambrian|Spelt with "Mt" in the text.||||||02-JUL-08
25287|Mount McDonnell Formation|22766|4|Described|Fig.2 p561, p563|Early Cambrian|Early Cambrian|Spelt Mt McDonnell Formation||||||
25287|Mount McDonnell Formation|22857|5|Briefly described|p88 Fig. 14.7A|Early Cambrian|Early Cambrian|Of the Kangaroo Island Group. Geological Province: Stansbury Basin. ||||||
25287|Mount McDonnell Formation|22858|6|Mentioned|Fig14.7ap88-9|Tommotian|Tommotian|||||||
25287|Mount McDonnell Formation|30377|6|Mentioned|p204|||Equivalent to Carrickalinga Head Formation||||||
25287|Mount McDonnell Formation|33471|6|Mentioned|Fig.1|||||||||
25287|Mount McDonnell Formation|42270|4|Described|p362|||||||||
25287|Mount McDonnell Formation|44133|5|Briefly described|p4 Fig. 7.2, 6, 9|Early Cambrian|Early Cambrian|Geological Province: Stansbury Basin. Of the Kanmantoo Group.||||||
25287|Mount McDonnell Formation|64282|5|Briefly described|Map legend|Early Cambrian|Early Cambrian|Of Kangaroo Island Group. In Stansbury Basin. Grey-green siltstone+ grey mudstone, variably calcareous. Starved ripples, linsen bedding, flaser bedding, ripple drift  x-lamination and bioturbation; Archaeocyaths in oolitic limestone. Mount is Mt in text.||||||24-JUL-08
25287|Mount McDonnell Formation|65375|5|Briefly described|p33.|Early Cambrian|Early Cambrian|||Unit in Kangaroo Island Group.||Overlies Kulpara Formation. Is overlain by Stokes Bay Sandstone.||
25287|Mount McDonnell Formation|65686|6|Mentioned|p411|Early Cambrian|Early Cambrian|Kangaroo Island.||||||
25287|Mount McDonnell Formation|65892|5|Briefly described|p9 Fig.4. |Early Cambrian|Early Cambrian|North Coast of Kangaroo Island.||||Is overlain by Stokes Bay Sandstone.||
25287|Mount McDonnell Formation|65921|6|Mentioned|p1, p2 (map legend).|Cambrian|Cambrian|||Of the Kangaroo Island Group.||||
25287|Mount McDonnell Formation|66761|5|Briefly described|p244, 246, 254|Cambrian|Cambrian|Not Present in PIRSA stratagraphic hole Investigator 1. Contains archaeocyaths, correlated with Fork Tree Limestone on Fleurieu Peninsula.||Base unit of the Kangaroo Island Group at Cape Cassini.||||14-MAR-12
25287|Mount McDonnell Formation|67344|6|Mentioned|p267|Cambrian|Cambrian|~30km west along the north coast of Kangaroo Island near Hummocky Point. Cambrian (series 2) unit.||||||
25287|Mount McDonnell Formation|69372|6|Mentioned|p27 fig. 5, p34 fig. 12|Cambrian|Cambrian|||Kangaroo Island Group||||
25287|Mount McDonnell Formation|73107|5|Briefly described|Map legend.|Early Cambrian|Early Cambrian|Stansbury Basin. Archaeocyaths in oolitic limestone.|||||Grey-green siltstone and grey-black mudstone, variably calcareous. Starved ripples, linsen bedding, flaser bedding, ripple drift cross-lamination and bioturbation.|
25287|Mount McDonnell Formation|73247|5|Briefly described|p204-207, p209|||[Written as Mt McDonnell Formation]. Part of the western succession of the Kangaroo Island Group. Contains burrows, trilobite tracks, possible mollusc trails and fragments of Redlichia.  Correlated with the Fork Tree Limestone based on archaeocyath assemblage from a thin oolitic limestone.||Kangaroo Island Group||Overlain by Stokes Bay Sandstone. Equivalent to Parara Limestone including Koolywurtie Member, and Kulpara Formation.||
25288|Mount Monster Porphyry|23869|5|Briefly described|p15 Fig. 3|Ordovician|Ordovician|||||||
25288|Mount Monster Porphyry|42275|6|Mentioned|Table 2 P474|||||||||
25288|Mount Monster Porphyry|44133|5|Briefly described|p51 Fig. 7.18, 56 Table 7.3|Ordovician|Ordovician|Acid Volcanics. Porphyritic rhyolite. A-Type. Age: 478 +/- 23Ma.||||||
25288|Mount Monster Porphyry|69372|6|Mentioned|p28|||Pebbles of this unit may be found in the Cape Jervis Formation.||||||
25288|Mount Monster Porphyry|73093|5|Briefly described|map legend|Ordovician|Cambrian||||||Rhyolite, quartz- and feldspar-phyric, orange-brown to grey-green, flow banded. A-type, post tectonic.|09-DEC-21
25293|Mount Schank Volcanic Complex|42097|6|Mentioned|p50|||||||||
27208|Mount Willoughby Limestone|24204|5|Briefly described|p263 Fig.4|Tertiary|Tertiary|||||||17-DEC-04
27208|Mount Willoughby Limestone|29658|6|Mentioned|p5|||||||||
27208|Mount Willoughby Limestone|30055|6|Mentioned|p153|||||||||
27208|Mount Willoughby Limestone|30807|6|Mentioned|p101|||Suggested map symbol||||||
27208|Mount Willoughby Limestone|30924|6|Mentioned|Map legend|Pliocene|Pliocene|||||||
27208|Mount Willoughby Limestone|31968|6|Mentioned|p8|||?Correlative Mangatitja Lst.||||||
27208|Mount Willoughby Limestone|32418|2|Defined|p1|Cenozoic|Cenozoic|See also p2.||||||12-JAN-16
27208|Mount Willoughby Limestone|32441|5|Briefly described|p123|||Ballast. Refers Nicol (1971) p173.||||||22-DEC-21
27208|Mount Willoughby Limestone|35080|6|Mentioned|p8|||||||||
27208|Mount Willoughby Limestone|38068|6|Mentioned|p76|||||||||
27208|Mount Willoughby Limestone|40003|5|Briefly described|Table 15|||||||||
27208|Mount Willoughby Limestone|40910|6|Mentioned|p18|||||||||
27208|Mount Willoughby Limestone|40911|6|Mentioned|Map legend|early Pleistocene|Miocene|Miocene - Early Pleistocene||||||
27208|Mount Willoughby Limestone|40925|6|Mentioned|Map legend|Cenozoic|Cenozoic|||||||19-NOV-08
27208|Mount Willoughby Limestone|40926|3|Fully described|p27|||||||||
27208|Mount Willoughby Limestone|41098|6|Mentioned|p177|||||||||
27208|Mount Willoughby Limestone|41165|6|Mentioned|p365|||||||||
27208|Mount Willoughby Limestone|42905|5|Briefly described|p23, Fig 5.3|||actually spelt Mt Willoughby Limestone||||||
27208|Mount Willoughby Limestone|64778|6|Mentioned|p13|Tertiary|Tertiary|Pedirka and Simpson Desert Basins.||||||
27208|Mount Willoughby Limestone|67120|5|Briefly described|Map legend|Pleistocene|Miocene||||||Cream, pale brown and pink calcareous rock with iron-stained clay and detrital quartz.|
27208|Mount Willoughby Limestone|70336|5|Briefly described|Map legend|Pleistocene|Miocene||||||Cream, pale brown and pink calcareous rock with iron-stained clay and detrital quartz.|12-JAN-16
36994|Mount Woods Complex|23480|5|Briefly described|p20 Fig 1|||||||||
36994|Mount Woods Complex|23481|5|Briefly described|p19 Fig 1|||Geological Province: Gawler Complex||||||
36994|Mount Woods Complex|23805|5|Briefly described|p4 Fig. 1|Paleoproterozoic|Paleoproterozoic|Geological Province: Gawler Craton.||||||07-NOV-08
36994|Mount Woods Complex|24505|5|Briefly described|p5 Fig. 1|||Geological Province: Gawler Craton.||||||
36994|Mount Woods Complex|60515|6|Mentioned|p116 Fig.1 |||||||||
36994|Mount Woods Complex|60953|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Age: >1736Ma (metamorphic age). Paragneiss, gneissic granitoids, basic dykes. Mount is Mt in text.||||||07-NOV-08
36994|Mount Woods Complex|61108|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|Spelt Mt on map legend. Paragneiss, gneissic granitoid rock and iron formation, granulite facies. Age: >1736 Ma (metamorphic age).||||||07-NOV-08
36994|Mount Woods Complex|61262|5|Briefly described|p455 Fig. 11|Paleoproterozoic|Paleoproterozoic|Age: <1800Ma. Geological Province: northern Gawler Craton. Mount is Mt in text of figure.||||||07-NOV-08
36994|Mount Woods Complex|61522|5|Briefly described|p5 Fig.1|||Geological Province: Gawler Craton.||||||
36994|Mount Woods Complex|61659|6|Mentioned|p30 Fig.1. |Paleoproterozoic|Paleoproterozoic||||||Paragneisses.|
36994|Mount Woods Complex|61864|6|Mentioned|p16 fig 3|||||||||
36994|Mount Woods Complex|62641|6|Mentioned|p277 Fig.1. |||||||||
36994|Mount Woods Complex|64722|6|Mentioned|Fig. 5 p.13|Paleoproterozoic|Paleoproterozoic|Of South Australian Craton.||||||
36994|Mount Woods Complex|64725|6|Mentioned|p58 Fig.2. |||Gawler Craton.||||||
36994|Mount Woods Complex|64739|6|Mentioned|p264 Fig.1. |Paleoproterozoic|Paleoproterozoic|Gawler Craton.||||||
36994|Mount Woods Complex|65376|6|Mentioned|p8 Fig.1.1. |Paleoproterozoic|Paleoproterozoic||||||Metasediments including iron-formation, granitic gneiss.|
36994|Mount Woods Complex|65390|6|Mentioned|p11 Fig.1, p22 Fig. 3|Statherian||Mount Woods Domain. Mount is spelt Mt in Fig. 3. Age >1740 Ma. ||||||
36994|Mount Woods Complex|65922|6|Mentioned|p13 Fig. 4|||Gawler Craton.||||||
36994|Mount Woods Complex|66302|5|Briefly described|p4 Fig.3, p20, p21, p32, p45, p76 Fig.20|||Mount Woods Domain, Gawler Craton. |||Includes the Skylark Metasediments, Coodnambana Metaconglomerate and the Engenina Adamellite.|Intruded by the Balta Granite.|Banded-iron formation, leucocratic gneiss, psammitic/pelitic schists and calcsilicates.|
36994|Mount Woods Complex|67112|6|Mentioned|p4 Fig.3|Mesoproterozoic|Mesoproterozoic|Gawler Craton.||||||
36994|Mount Woods Complex|67536|5|Briefly described|Map Legend|Calymmian|Calymmian|Gawler Craton. Coober Pedy Ridge metamorphism 1565 +/- 8 Ma and inheritance ~1750 Ma.|ca. 1565 +/- 8 Ma; inheritance ~ 1750 Ma||||Granulite-grade paragneiss, often iron-rich, felsic granulite; precursor of unknown age.|
36994|Mount Woods Complex|68131|5|Briefly described|p2 Fig.1|Paleoproterozoic|Paleoproterozoic||||||Metasediments including iron formation, and granitic gneiss.|
36994|Mount Woods Complex|69649|6|Mentioned|p6 Fig.4,||||||||Includes paragneisses.|
36994|Mount Woods Complex|72488|6|Mentioned|p2 Fig.1|||Eastern Gawler Craton.|1.75 Ga.|||||
36994|Mount Woods Complex|72725|6|Mentioned|p41, p43-44|Statherian|Statherian|Max age date is maximum depositional ages. Min  age is from igneous component (assume crystallisation age). Metamorphism age of ~1736 Ma.|~1750 Ma, 1691 Ma||||Paragneiss, psammitic, pelitic, magentite-bearing, calc-silicate, BIF, metaconglomerate; orthogneiss, granitic; amphibolite; monzogranite, foliated.|
36994|Mount Woods Complex|73155|6|Mentioned|p266|||Mount Woods Domain. See also Mount Woods Metamorphic Complex p276, Mount Woods Metamorphics p285.|||Skylark Metasediments, Mount Woods Metamorphics, Engenina Adamelite, Coodnambana Metaconglomerate, Balta Granite Suite, Mirage Granite.|||05-SEP-22
28822|Mt Remarkable Quartzite|29780|6|Mentioned|p12|||||||||
68775|Muckanippie Suite|60953|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Anorthosite, gabbro, diorite.||||||07-NOV-08
68775|Muckanippie Suite|61108|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|Anorthosite, gabbro and diorite.||||||07-NOV-08
68775|Muckanippie Suite|65385|6|Mentioned|pS128 Fig. 2|||Anorthosite, gabbro and diorite.||||||08-MAR-12
68775|Muckanippie Suite|67536|6|Mentioned|Map Legend|||Gawler Craton.|Uncertain age.||||Anorthosite, gabbro, diorite.|
68775|Muckanippie Suite|68131|6|Mentioned|p77|Paleoproterozoic|Paleoproterozoic|||||||
28826|Mulgathing Complex|22613|4|Described|p10|Proterozoic|Archean|||||||07-NOV-08
28826|Mulgathing Complex|22614|5|Briefly described|map|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
28826|Mulgathing Complex|22629|4|Described|fig2 p147, 148|Archean|Archean|||||||07-NOV-08
28826|Mulgathing Complex|22838|6|Mentioned|P12||Archean|||||||07-NOV-08
28826|Mulgathing Complex|23124|6|Mentioned|p397|||||||||
28826|Mulgathing Complex|23175|6|Mentioned|p5||Archean|||||||07-NOV-08
28826|Mulgathing Complex|23481|5|Briefly described|p19 Fig 1|Archean|Archean|Geological Province: Gawler Craton.||||||07-NOV-08
28826|Mulgathing Complex|23731|5|Briefly described|p43, p51|Archean|Archean|Geological Province: Gawler Craton.||||||07-NOV-08
28826|Mulgathing Complex|23805|5|Briefly described|p4 Fig. 1|Archean|Archean|Geological Province: Gawler Craton.||||||07-NOV-08
28826|Mulgathing Complex|24261|5|Briefly described|p1047 Fig.1|Archean|Archean|Geological Province: Gawler Craton.||||||07-NOV-08
28826|Mulgathing Complex|24296|5|Briefly described|p1250|Archean|Archean|Geological Province: Gawler Craton.||||||07-NOV-08
28826|Mulgathing Complex|24422|6|Mentioned|p84 Fig. 1|Archean|Archean|Geological Province: Gawler Craton.||||||07-NOV-08
28826|Mulgathing Complex|24472|5|Briefly described|p5 Tb.1|Archean|Archean|Geological Province: Harris Greenstone Domain, Gawler Craton.||||||07-NOV-08
28826|Mulgathing Complex|24505|5|Briefly described|p8|Archean|Archean|Includes Kenella Gneiss and Glenloth Granite. Geological Province: Gawler Craton.||||||07-NOV-08
28826|Mulgathing Complex|24511|5|Briefly described|p56|Archean|Archean|Comprising metamafics, ultramafics, granites, mafic gneisses and possible greenstones.||||||07-NOV-08
28826|Mulgathing Complex|24526|5|Briefly described|p95,p98|Paleoproterozoic||Geological Province: Gawler Craton.||||||07-NOV-08
28826|Mulgathing Complex|24597|5|Briefly described|p526 Fig. 1|Archean|Archean|Age: ca2640-2300Ma. Geological Province: Gawler Craton. See also p525.||||||23-SEP-14
28826|Mulgathing Complex|38604|6|Mentioned|Map legend|Paleoproterozoic|Archean|Archaean - Early Proterozoic||||||07-NOV-08
28826|Mulgathing Complex|38605|4|Described|p13|||See also Table 2.||||||
28826|Mulgathing Complex|39352|6|Mentioned|Map legend|Proterozoic|Archean|||||||07-NOV-08
28826|Mulgathing Complex|39802|6|Mentioned|Map legend|Paleoproterozoic|Archean|||||||07-NOV-08
28826|Mulgathing Complex|40644|4|Described|p120 Fig. 2, p123,  p126|Paleoproterozoic|Archean|Comprises Glenloth Granite, Kenella Gneiss and Christie Gneiss. Geological province: Gawler Craton. See also p124 Fig. 3.||||||07-NOV-08
28826|Mulgathing Complex|40912|6|Mentioned|Map legend|Paleoproterozoic|Archean|Archaean-Early Proterozoic||||||07-NOV-08
28826|Mulgathing Complex|40942|6|Mentioned|p8|||||||||
28826|Mulgathing Complex|41402|6|Mentioned|p35|||||||||
28826|Mulgathing Complex|41493|6|Mentioned|Table 1|||||||||
28826|Mulgathing Complex|41609|5|Briefly described|p126|||See also Fig.3||||||
28826|Mulgathing Complex|41972|6|Mentioned|p365|||||||||
28826|Mulgathing Complex|42102|6|Mentioned|p85|||||||||
28826|Mulgathing Complex|42357|5|Briefly described|p8|||||||||
28826|Mulgathing Complex|42465|5|Briefly described|Map Legend|||||||||
28826|Mulgathing Complex|42466|5|Briefly described|Map Legend|||||||||
28826|Mulgathing Complex|42468|5|Briefly described|p13|||||||||
28826|Mulgathing Complex|42469|3|Fully described|p7|||||||||
28826|Mulgathing Complex|42475|6|Mentioned|p10|||||||||
28826|Mulgathing Complex|42546|5|Briefly described|Map legend|Paleoproterozoic|Archean|||||||07-NOV-08
28826|Mulgathing Complex|42736|5|Briefly described|map legend|Paleoproterozoic||||||||07-NOV-08
28826|Mulgathing Complex|42816|4|Described|p11|||||||||
28826|Mulgathing Complex|43052|4|Described|p38,Table 3.2|||||||||
28826|Mulgathing Complex|43053|5|Briefly described|Map Legend|Paleoproterozoic|Archean|Metasedimentary and granitic gneiss, amphibolite (including pillow basalt, pyroxenite, komatiite); granitoids. Geological Province: northern Gawler Craton.||||||07-NOV-08
28826|Mulgathing Complex|43071|5|Briefly described|p9|||||||||
28826|Mulgathing Complex|43094|5|Briefly described|Table 1.|||||||||
28826|Mulgathing Complex|43141|6|Mentioned|p63,Fig.1||Archean|||||||07-NOV-08
28826|Mulgathing Complex|43258|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
28826|Mulgathing Complex|43298|5|Briefly described|Map Legend|Paleoproterozoic|Archean|||||||07-NOV-08
28826|Mulgathing Complex|43561|6|Mentioned|p1434|||||||||
28826|Mulgathing Complex|43839|5|Briefly described|Fig2 p30||Paleoproterozoic|||||||12-JUL-16
28826|Mulgathing Complex|44695|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
28826|Mulgathing Complex|44935|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
28826|Mulgathing Complex|50130|5|Briefly described|p2|Archean|Archean|Age: 3150 - 2950 Ma. Geological Province: Gawler Craton.||||||07-NOV-08
28826|Mulgathing Complex|60484|5|Briefly described|p33 Fig. 1|||Geological Province: Gawler Craton.||||||
28826|Mulgathing Complex|60515|6|Mentioned|p116 Fig.1 |||||||||
28826|Mulgathing Complex|60704|5|Briefly described|p686 Fig.1, p697|Paleoproterozoic|Archean|Intrudes the Kenella Gneiss. Geological Province: Gawler Craton.||||||07-NOV-08
28826|Mulgathing Complex|60953|5|Briefly described|Map Legend|Archean|Archean|Age: 2440-2400 Ma (metamorphic age).||||||07-NOV-08
28826|Mulgathing Complex|60954|5|Briefly described|Map Legend|Archean|Archean|Geological Province: Gawler Craton.||||||
28826|Mulgathing Complex|61108|5|Briefly described|map legend|Archean|Archean|Paragneiss, granitic orthogneiss, iron formation and mafic granulite, granulite to amphibolite facies. Age: >2440-2400 Ma (metamorphic age).||||||07-NOV-08
28826|Mulgathing Complex|61393|5|Briefly described|p165, p167, p170, p176.  |Early Paleoproterozoic|Late Archean|Central Gawler Craton. Separated from the Tunkillia and St. Peter Suites by the Yerda Shear Zone.|c.2560 - 2400 Ma.||||Granulites.|
28826|Mulgathing Complex|61522|5|Briefly described|p5 Fig.1|||Geological Province: Gawler Craton.||||||
28826|Mulgathing Complex|61659|5|Briefly described|pp28-31, p37, p38, p40.    |Paleoproterozoic|Archean |Gawler Craton. Has low magnetization intensity.|||Includes Christie Gneiss.|Intruded by the Hiltaba Suite.||
28826|Mulgathing Complex|61836|5|Briefly described|p208|Archean|Archean|Metasediments - kaolin and kaolin-quartz rocks, foliated, non-foliated, and very fine to very coarse-grained, and quartz reefs and stringers. Geological Province: Gawler Craton.||||||07-NOV-08
28826|Mulgathing Complex|61864|6|Mentioned|p16 fig 3|Archean|Archean||||||Orthogneiss and paragneiss.|
28826|Mulgathing Complex|62641|6|Mentioned|p277 Fig.1. |||||||||
28826|Mulgathing Complex|62893|6|Mentioned|p26|Palaeoproterozoic|Late Archaean|Intruded by granitoids during the Sleafordian Orogeny (2500-2300 Ma).|||||[Metamorphosed] volcanic and sedimentary rocks.|
28826|Mulgathing Complex|62978|5|Briefly described|p161|||Interlayered granulite-facies para- and orthogneisses. Geological Province: Gawler Craton.||||||07-FEB-11
28826|Mulgathing Complex|63020|5|Briefly described|p971|Archean|Archean|Geological Province: Gawler Craton.||||||07-NOV-08
28826|Mulgathing Complex|63067|5|Briefly described|p2 Fig. 1|Archean|Archean|Granite, orthogneiss, amphibolite, metasediments.||||||07-NOV-08
28826|Mulgathing Complex|63223|5|Briefly described|p17 Fig. 1|Archean|Archean|Geological Province: Gawler Craton.||||||07-NOV-08
28826|Mulgathing Complex|63275|5|Briefly described|p13, p14 Fig.1, p18, p20.|Archean|Archean|Oldest parts of Gawler Craton. Metamorphosed by early Paleoproterozoic Sleafordian Orogeny.||||||
28826|Mulgathing Complex|63866|5|Briefly described|p3, p17, p22|Early Proterozoic|Archaean||c. 2450 Ma||Includes the Christie Gneiss.|Overlain by the Wilgena Hill Jaspilite. Equivalent to the Sleaford Complex.||
28826|Mulgathing Complex|64130|6|Mentioned|p1378 Fig.1, p1379, p1380 Fig.2|Paleoproterozoic|Archean|Central-western Gawler Craton. Shares common history with Sleaford Complex. Includes calc-alkaline volcanics dated at 2558 +/- 6 Ma (Cowley and Fanning, 1991).|~2550-2440 Ma.||||Aluminous metasediments interlayered with BIFs, carbonates, and siliceous rocks, with broadly coeval felsic and mafic-ultramafic volcanics including komatiites.|
28826|Mulgathing Complex|64131|5|Briefly described|p1399 Fig.2, p1401, p1404  |Archean|Archean|Petrophysical properties.|2900? to 2430 Ma|||Correlated with the Sleaford Complex||
28826|Mulgathing Complex|64137|5|Briefly described|p1542 Fig.1, p1543, |Archean|Archean||||Includes the Kenella Gneiss and Glenloth Granite.|||
28826|Mulgathing Complex|64313|5|Briefly described|p451 Fig.a|||Geological province: Gawler Craton.||||||09-FEB-10
28826|Mulgathing Complex|64573|5|Briefly described|p779, p780 Fig. 1|Mesoproterozoic|Neoarchean|Geological Province: Gawler Craton. Contain metamorphosed felsic to intermediate volcanic and sedimentary rocks emplaced or deposited between 2600 and 2500Ma.||||||07-FEB-11
28826|Mulgathing Complex|64722|5|Briefly described|Fig. 2 p3-6, p12, 24, 27|Siderian||Northwest Gawler Province. Minimum age from intrusion at 2500 Ma.||||Intruded by Glenloth Granite.|Banded iron formation, carbonate, calc-silicate, quartzite and aluminous sedimentary rocks.|11-APR-12
28826|Mulgathing Complex|64739|6|Mentioned|p264 Fig.1, p266, p280.|Archean|Archean|Gawler Craton.|c.2450 Ma.||Includes Christie Gneiss.|||
28826|Mulgathing Complex|64740|6|Mentioned|p284 Fig.1. |Archean|Archean|||||||
28826|Mulgathing Complex|64741|5|Briefly described|p299 Fig. 2|Archean|Archean|Age: 2550-2500Ma.||||||07-FEB-11
28826|Mulgathing Complex|64828|5|Briefly described|p1064 Fig. 1|Archean|Archean|Geological province: Gawler Craton.||||||04-MAR-09
28826|Mulgathing Complex|65376|4|Described|p8 Fig.1.1, p169, pp190-197.|Paleoproterozoic|Archean|Northern Gawler Craton. The c.2500-2400 Ma Sleafordian Orogeny produced NE-trending, tight to isoclinal folding and granulite facies metamorphism. Shares many similarities with Sleaford Complex; they may have been one continuous belt.|||Includes Hopeful Hill Basalt, Lake Harris Komatiite, Christie and Kenella Gneisses, Blackfellow Hill Pyroxenite, South Lake Gabbro, Glenloth Granite, Aristarchus Peridotite and Mobella Tonalite.||Banded iron-formation, quartz and feldspar-rich ortho- and paragneisses with mafic and ultramafic rocks, mafic and felsic volcanics.|
28826|Mulgathing Complex|65385|4|Described|pS128 Fig.2, pS131 Tab.2, pS132, pS135|Siderian|Neoarchean|Metasedimentary rocks, granite, tonalite, gneiss, gabbro, pyroxenite, peridotite and komatiite. 2560-2440 Ma. In the northern and central Gawler Craton. Includes Christie Gneiss, Blackfellow Hill Pyroxenite and Mobella Tonalite.||||||08-MAR-12
28826|Mulgathing Complex|65390|5|Briefly described|p14, p22 Fig. 3|Archean|Archean|Age >2500 Ma. Intruded by ~1690 - 1670 Ma intrusives. Includes Christie Gneiss and Kenella Gneiss. Low magnetic intensity. Hosts Challenger gold deposit.||||||
28826|Mulgathing Complex|65483|6|Mentioned|p17 Fig. 1|Archean|Archean|||||||
28826|Mulgathing Complex|65485|6|Mentioned|Fig 1|Archean|Archean|||||||
28826|Mulgathing Complex|65772|6|Mentioned|p229 Fig.2|Paleoproterozoic|Archean|||||||
28826|Mulgathing Complex|65915|5|Briefly described|p1-2, p3 Fig.2, p18, p20|Siderian|Neoarchean|Gawler Craton basement. ~2550-2430 Ma. Protoliths to these gneisses include late Archean sediments and intercalated volcanics aged ~2550 -2500 Ma. Metamorphosed during Sleaford Orogeny (~2500-2400 Ma).||||||
28826|Mulgathing Complex|65922|6|Mentioned|p13 Fig. 4|||Gawler Craton.||||||
28826|Mulgathing Complex|66302|5|Briefly described|p4 Fig.3, p10-p12, p22, p55, p84|Paleoproterozoic|Neoarchean|Christie Domain, Gawler Craton. Rocks of this Complex were metamorphosed to granulite facies during the 2480-2420 Ma Sleafordian Orogeny. |||Includes the Christie Gneiss, Kenella Gneiss, Devils Playground Volcanics, Lake Harris Komatiite, Hopeful Hill Basalt, South Lake Gabbro and the Glenloth Granite.|Overlain by the Wilgena Hill Jaspilite.|Metasedimentary rocks.|
28826|Mulgathing Complex|66882|6|Mentioned|p101 Fig.1, p116-117, p120|Neoarchean|Neoarchean|Gawler Craton. Possible source rocks for c.2500 Ma zircons in Cleve Group.||||||
28826|Mulgathing Complex|67058|5|Briefly described|p476, p480 Fig.4, p490, p491, p492.|Neoarchean|Neoarchean|Central Gawler Craton.|||Includes Christie Gneiss, Kenella Paragneiss, Harris Greenstone Belt, Devils Playground Volcanics and Glenloth Granite.|||
28826|Mulgathing Complex|67112|6|Mentioned|p4 Fig.3|Archean|Archean|Gawler Craton.||||||
28826|Mulgathing Complex|67181|5|Briefly described|p616 Fig.1, p630|Archean|Archean|Gawler Craton. Possible northerly continuation of the Complex in the central Gawler Craton, forming a deep basement to the northern Gawler Craton. References: Fairclough et al. 2003, Payne et al. 2003.||||||
28826|Mulgathing Complex|67536|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Gawler Craton. Informally subdivided into two parts.|ca. 2553 +/- 9 Ma||||Rhyodacite, andesite and minor basalt (ALm1); paragneiss, granitic orthogneiss, iron formation, mafic granulite (ALm).|
28826|Mulgathing Complex|67721|6|Mentioned|p36||||||Includes the Devils Playground Volcanics.|||
28826|Mulgathing Complex|67980|6|Mentioned|p550|Proterozoic|Archean|Christie Domain, northwest Gawler Craton. Deformed and metamorphosed during Sleafordian Orogeny, between ca 2470 and 2410 Ma.|||||Gneisses.|
28826|Mulgathing Complex|68128|5|Briefly described|p1-p2, p5, p7-10, p19, p28,|Palaeoproterozoic|Archaean|Gawler Craton. Deformed, metamorphosed and intruded by syn-tectonic felsic and mafic intrusions during the 2460-2420 Sleafordian Orogeny. Covers an area of more than 6000 km^2. Outcrop is poor, discontinuous and structurally complex. Prospective for a range of commodities including gold, nickel, copper, PGE and iron ore. See also p42-43, p53, p58, p64-65, p73, p77, p83, p91, p100.|ca 2555-2510 Ma||Includes the South Lake Gabbro, Hopeful Hill Basalt, Kenella Gneiss, Lake Harris Komatiite, Glenloth Granite, Christie Gneiss, Aristarchus Peridotite, Blackfellow Hill Pyroxenite, Mobella Tonalite.||Felsic and mafic to ultramafic volcanic rocks and clastic and chemical sediments including banded iron formation and quartz- and feldspar-rich ortho- and paragneisses.|01-FEB-23
28826|Mulgathing Complex|68131|5|Briefly described|p2 Fig.1, p77, p96|Paleoproterozoic|Archean|Associated with Sleafordian Orogeny. Mapped with Sleaford Complex as a single unit.|~2550-2440 Ma.||||Metasedimentary and felsic and mafic gneiss to granulite, including iron formation.|
28826|Mulgathing Complex|68208|5|Briefly described|p31, p35, p37 Fig.10|Paleoproterozoic|Neoarchean|Affected by the 2470 - 2420 Ma Sleafordian Orogeny.|2555 - 2450 Ma||Includes Christie Gneiss, Kenella Gneiss, Mobella Tonalite, Devils Playground Volcanics, Glenloth Granite||Volcanosedimentary and plutonic rock association.|
28826|Mulgathing Complex|69004|5|Briefly described|p15, p18, p39|Palaeoproterozoic|Archean|Gawler Craton. Hosts a regional watertable aquifer.|||||Variety of rocks including banded iron formations, chert and aluminous metasedimentary rocks. Meta-igneous bodies, komatiites and basalts also occur.|
28826|Mulgathing Complex|69048|5|Briefly described|p1, p18|||Central Gawler Craton. |||Christie Gneiss.|Correlative of Sleaford Complex.||
28826|Mulgathing Complex|69203|5|Briefly described|p9, p22, p34-37|||Daly and Fanning (1993).|c.2555-2415 Ma.||||Metasedimentary and meta-igneous gneisses.|
28826|Mulgathing Complex|69213|5|Briefly described|p29, 24, 30|Paleoproterozoic|Neoarchean|Gawler Craton. Metamorphosed in Sleafordian Orogeny.|2555-2420 Ma||Includes Christie Gneiss|Considered lateral equivalent of Sleaford Complex.|Comprises lithologies ranging from ultramafic intrusions and komatiite, basaltic and felsic volcanics to clastic and chemical sediments, together with a range of felsic-mafic intrusions.|
28826|Mulgathing Complex|69554|6|Mentioned|p127-128, 130, 136, 140|Paleoproterozoic|Neoarchean|Central Gawler Craton, S of the Karari Shear Zone. Forms basement, which is inferred to be at least in part derived from Mesoarchean crust.|c.2555-2415 Ma.||||Metasedimentary and meta-igneous gneisses.|
28826|Mulgathing Complex|69595|5|Briefly described|p37|Neoarchean|Neoarchean|Gawler Craton. Interpreted to have formed by interaction of a convergent margin and mantle plume with the sedimentary component having deposited in a back-arc or arc-rift basin setting.|c. 2560-2500 Ma||||Metasedimentary rocks and generally coeval felsic and mafic to ultramafic volcanic rocks.|
28826|Mulgathing Complex|69648|4|Described|p10 Fig.4,p12 Fig.6,p13,p34, map legend|Archean|Archean|Christie Subdomain, western Gawler Craton. Occurrences on adjacent sheets have been subdivided into several Formation and Members, including paragneisses of the Christie Gneiss. Misspelled in Figure 4 as Malgathing Complex.|||Christie Gneiss|Intruded by Ifould Complex.|Paragneiss and orthogneiss; undifferentiated, predominantly felsic metasediments, including leucocratic gneiss and granulite.|
28826|Mulgathing Complex|69649|5|Briefly described|p6 Fig.4, p35, p58|Archean|Archean|Western Gawler Craton. Deformed by Sleafordian Orogeny.|||Includes Glenloth Granite.|||
28826|Mulgathing Complex|70023|6|Mentioned|p182|||Geological province: Gawler Craton.||||||
28826|Mulgathing Complex|70027|5|Briefly described|p57,71|Paleoproterozoic|Neoarchean|Geological province: Gawler Craton. Contains ca. 2560 Ma magmatic rocks (Devils Playground Volcanics? p71).||||Interlayered with Christie Gneiss.|Migmatised metasedimentary gneisses.|
28826|Mulgathing Complex|70286|6|Mentioned|p884|||Eastern Gawler Craton.||||||
28826|Mulgathing Complex|70337|5|Briefly described|Map legend.|Paleoproterozoic|Archean||||||Granite, tonalite, gneiss, gabbro, basalt, pyroxenite, peridotite, komatiite.|
28826|Mulgathing Complex|70405|6|Mentioned|p12 figure 4|Paleoproterozoic|Archean||2500 Ma|||||
28826|Mulgathing Complex|70511|6|Mentioned|p87, 96, 98|Archean|Archean|Gawler Craton.|2500 Ma.|||||
28826|Mulgathing Complex|70778|6|Mentioned|p1|||||||||
28826|Mulgathing Complex|70789|5|Briefly described|p316, p319|||Crystalline basement to the Gawler Craton.|c.2555-2440 Ma.|||Is overlain by the Tarcoola Formation.|Gneisses: metamorphosed clastic and chemical sedimentary rocks, metavolcanics, and multiple syn-sedimentary intrusions.|
28826|Mulgathing Complex|70893|6|Mentioned|p3 fig 1a||||c. 2555 - 2410 Ma|||||05-SEP-19
28826|Mulgathing Complex|70947|6|Mentioned|p960|Paleoproterozoic|Archean|Geological province: Gawler Craton.|ca. 2555-2410 Ma|||||
28826|Mulgathing Complex|71043|5|Briefly described|p104, p106-107, p115, p117|Neoarchean|Neoarchean|North-central Gawler Craton. Underwent high-grade metamorphism and deformation during the c.2470-2420 Ma Sleaford Orogeny; moreso in the west and central parts than in the east. Tonalite from drillhole SH 7 was dated at 2529 +/- 6 Ma, contemporary with Hall Bay Volcanics.|c.2555-2410 Ma.||Devils Playground Volcanics.||Hematite-altered tonalite. Mostly gneissic from upper amphibolite to granulite facies metamorphism.|
28826|Mulgathing Complex|71236|5|Briefly described|p2|Archean|Archean|||||||
28826|Mulgathing Complex|71322|6|Mentioned|p91|Paleoproterozoic|Neoarchean||c.2560-2440 Ma.|||||
28826|Mulgathing Complex|71341|6|Mentioned|p179 fig 1, p180-p181, p192, p196, p198|Palaeoproterozoic|Neoarchean|Christie Domain, Gawler Craton. |ca. 2555-2410 Ma||||Gneiss.|
28826|Mulgathing Complex|71348|6|Mentioned|p201|Paleoproterozoic|Archean|Geological province: Gawler Craton.||||||
28826|Mulgathing Complex|71534|6|Mentioned|p295-p296|Paleoproterozoic|Neoarchean|Geological province: Gawler Craton.||||||
28826|Mulgathing Complex|71536|6|Mentioned|p137, p141-142||||||Includes the Kenella Gneiss.|||
28826|Mulgathing Complex|71559|6|Mentioned|p16 fig 2|||Geological province: Gawler Craton.||||||
28826|Mulgathing Complex|71712|5|Briefly described|P410|Archean|Archean|Sedimentary and felsic to ultramafic volcanic protoliths, and felsic to intermediate plutonic rocks metamorphosed during Sleafordian Orogeny around 2450 Ma||||||31-MAR-20
28826|Mulgathing Complex|71859|4|Described|p2-p3, p7, p17, p24, p26, p28|||Northern Gawler Craton. Lithologically similar to the Sleaford Complex. The majority of this unit underwent granulite facies metamorphism during the Sleafordian Orogeny (2475-2410 Ma).|||Includes the Devil's Playground Volcanics, Lake Harris Komatiite, the Christie Gneiss and the Kenella Gneiss.|Overlies the Cooyerdoo Granite and the Coolanie Gneiss.||05-APR-23
28826|Mulgathing Complex|71862|6|Mentioned|p3-p4|||Northern Gawler Craton.||||||
28826|Mulgathing Complex|72090|6|Mentioned|p11|Paleoproterozoic|Neoarchean|Olympic Domain, Gawler Craton.||||||
28826|Mulgathing Complex|72242|6|Mentioned|p27|Siderian|Neoarchean|Geological province: Coompana Province, Western Gawler Craton. Pre-dates Sleafordian Orogeny.||||||
28826|Mulgathing Complex|72462|6|Mentioned|p3|Archean|Archean|Gawler Craton.||||||
28826|Mulgathing Complex|72725|6|Mentioned|p41, p43-44|Siderian|Neoarchean|Age range represents protoliths.|~2560-2460 Ma||||Paragneiss, arenaceous and aluminous; iron formation; granitic gneiss; felsic and mafic-ultramafic volcanic and intrusive rocks. Granulite to amphibolite facies.|
28826|Mulgathing Complex|72949|6|Mentioned|p34|Siderian|Neoarchean||ca. 2.555-2.410 Ga|||||
28826|Mulgathing Complex|73026|5|Briefly described|p4 fig1.2, p5|early Paleoproterozoic|Neoarchean|Occurs in the central Gawler Craton. The oldest component of this complex was protolith to the Coolanie Gneiss.|c. 2560-2440 Ma|||Underlies the Gawler Range Volcanics.||
28826|Mulgathing Complex|73027|5|Briefly described|p4, p10|Palaeoproterozoic|Neoarchaean|Deformed by the Sleafordian orogeny at c. 2465-2410 Ma.||||||
28826|Mulgathing Complex|73030|6|Mentioned|p2148-2149, p2151|Siderian|Neoarchean|Gawler Craton.|ca. 2555 - 2410 Ma|||||
28826|Mulgathing Complex|73112|5|Briefly described|Map legend.|||Shown in the Solid Geology Interpretation map, below the main Nullarbor 250k map.||||||
28826|Mulgathing Complex|73155|5|Briefly described|p274, p277, p282 Fig.13, p283, p285 Tb.1|Siderian|Neoarchean|Gawler Craton. Faulted against Paleo- to Mesoproterozoic metasedimentary and igneous rocks of the Mount Woods Domain. Generally low magnetic and Bouguer gravity response. Location in text includes p264 Fig.1.|ca. 2555-2410 Ma||Christie Gneiss||Banded iron formation, marble, calc-silicate gneiss, cordierite gneiss, granitic gneiss and garnetiferous migmatic gneiss.|
28826|Mulgathing Complex|73162|6|Mentioned|p449, Fig.1|||||||||
28826|Mulgathing Complex|73165|6|Mentioned|p621|Paleoproterozoic|Neoarchean|Gawler Craton, central western. Formed from basin development, bimodal magmatism and sedimentation. Basin deveopment terminated in the Sleafordian Orogeny ca 2480-2420 Ma.||||||
28826|Mulgathing Complex|73166|6|Mentioned|p644|Neoarchean|Neoarchean|Gawler Craton, eastern.|ca 2.5 Ga|||||
28826|Mulgathing Complex|73230|3|Fully described|p4-10, p12-15|earliest Paleoproterozoic|Archean|Gawler Craton, central. Comprises a series of elongate, northeast-trending fault-bound blocks. Due to diverse lithologies, it has the potential to host a diverse set of mineral commodities, including gold, nickel-copper-platinum group elements (PGE) and iron (magnetite). Gold mineralisation occurs in metamorphosed and vein-hosted styles, and possibly others. Mostly undergone amphibolite to granulite facies metamorphism during the Sleafordian Orogeny (c. 2475-2390 Ma) except in the eastern region. Originally defined by Daly (1986); named after Mulgathing Homestead northeast of Tarcoola (see historical review by Reid and Daly, 2009). Original definition included 10 units; this study includes 14 formal units and other undifferentiated rocks. Different lithostratigraphic packages tend to occur in different areas with limited overlap; the three main areas are undifferentiated Gawler Craton/eastern Mulgathing Complex, Harris Greenstone Domain, and the Christie and Wilgena domains. Contains at least three suites/sequences of mafic-ultramafic rocks.  Dominated by felsic lithologies with low magnetic response. Lithologies with very similar mineralogy but varied protoliths makes the identification of stratigraphic units within the complex challenging, particularly with poor and sporadic outcrop and relatively sparse diamond drilling. Correlation is currently made through geochronology. More constituents: Burden Metagabbro, Christie Gneiss, George Hill Iron Member, Aurora Tank Suite, Aristarchus Metaperidotite, Skuse Hill Metapyroxenite.|||Devils Playground Volcanics, Sloan Hill Tonalite, Lake Harris Komatiite, Hopeful Hill Basalt, South Lake Gabbro, Kenella Gneiss, Glenloth Granite, Mobella Tonalite, and more [see comments].||Diverse set of metamorphosed and deformed lithologies including komatiite, gabbro, amphibolite, tonalite and other granitoids, volcanic and volcaniclastic lithologies, and metasedimentary schists to migmatitic gneisses.|
28826|Mulgathing Complex|73233|6|Mentioned|p27 Fig.1, p28|Siderian|Neoarchean|Gawler Craton. Western Fowler Domain, crops out in vicinity of Lake Ifould. Late Archean to earliest Paleoproterozoic.|||||Granitic magmatism and undifferentiated clastic sediment.|
28826|Mulgathing Complex|73235|6|Mentioned|p52-53, p55-56|Siderian|Neoarchean|Gawler Craton. Christie and Gawler Range Volcanic regions. Hosts Challenger; Golf Bore and Aurora Tank orogenic gold mineralisation.|c. 2555-2410 Ma|||||
28826|Mulgathing Complex|73298|6|Mentioned|p1072 Fig.1, p1073, p1078 Fig.6|Neoachean|Neoarchean|Gawler Craton, central-western. Nawa, Christie and Coulta domains. Represents volcano-sedimentary basins terminated during and deformed by the 2480-2420 Ma Sleafordian Orogeny.|ca 2550 Ma|||||
28826|Mulgathing Complex|73302|6|Mentioned|p53|Neoarchean|Neoarchean|Despite being adjacent to, or within close proximity of, the St Peter Suite, there are no inherited Archaean zircons in the latter.||||||
28826|Mulgathing Complex|73493|6|Mentioned|p714 Fig.1, p716 Fig.3|Siderian|Neoarchean|Gawler Craton.|c.2555-2410 Ma|||||
28826|Mulgathing Complex|74361|6|Mentioned|p163|||Central-northern Gawler Craton. Deformed by the Sleafordian (~2480-2420 Ma) and Kimban (~1730-1690 Ma) Orogenies.|~2500 Ma.|||||
34081|Mullamullang Member|22613|5|Briefly described|p22|||||||||
34081|Mullamullang Member|22626|4|Described|438|Middle Miocene|Middle Miocene|Geol province: Eucla Basin. Parent Nullarbor Limestone. Age from foraminifera fauna.||||||14-SEP-18
34081|Mullamullang Member|44133|5|Briefly described|p180, 184|Miocene|Miocene|Geological Province: Eucla Basin. Of the Nullarbor Limestone. ||||||
34081|Mullamullang Member|62640|5|Briefly described|pp70-71, p72 Fig.6, p73. |Miocene|Miocene||c.20 Ma.|Unit in Nullarbor Limestone.||Of the Nullarbor Limestone|Nodular algal limestone.|
34081|Mullamullang Member|70397|4|Described|p2-5,7-8,11,14|Middle Miocene|Middle Miocene|Eucla Basin. Depositional environment: calm shelf, water depths 15-30m. Maximum thickness: 8m. Entirely comprises of the Rhodolith Facies.||Unit of Nullabor Limestone.||Basal unit of Nullabor Limestone. Overlain by/interbedded with Rawlinna member. Underlain by Wilson Bluff Limestone.|Rhodolith rudstone and floatstone with an articulated branching coralline algae, small benthic foraminifera and echinoderm-fragment grainstone and packstone matrix.|
34081|Mullamullang Member|70771|4|Described|p4, p31, p53-p58, p60-p61|||Eucla Platform, Eucla Basin. Attains a maximum thickness of 10m along the Hampton Range. It is interpreted to represent a transgressive rhodolith gravel deposit typical of those that form in the lower photic zone.||Nullarbor Limestone||Overlain by the Rawlinna Member.|Algal limestone with floatstone and rudstone textures.|
34081|Mullamullang Member|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||limestone rudstone|
34081|Mullamullang Member|71361|5|Briefly described|p34, p80, p119|||Paleoenvironment discussed in detail. See also p122, p127, p129, p142, p144, p146-p147, p152.|||||Rhodolith rudstones and floatstones with articulated coralline algae fossils and echinoderm fragment grainstone and packstone matrix.|
22467|Mulligan Dam Regolith|68068|5|Briefly described|Map legend|Paleocene|Paleocene|Callabonna Sub-basin, Lake Eyre Basin.||||Is overlain by Eyre Formation.|Basal pallid blotchy to mottled red pedolith to saprolith zone to 2 m thick; then massive to indistinctly bedded gravelly to pebbly sandstone < 5 m thick with well-rounded silcrete pebbles, yellow-grey to yellow-brown, exhibits cavernous weathering.|
22467|Mulligan Dam Regolith|69023|4|Described|p87, p107, p109-112, p114-116, p120-123|Paleocene|Paleocene|New name (Sheard and Alley, 2009); after Mulligan Dam, 12km NE of Moolawatana homestead. Type area 4km W of Mulligan Dam detailed with a composite profile. Has appeared on previous maps as 'silcreted Murnpeowie Formation'. Bleaching and colluvium.||||Overlies Marree Subgroup. Is overlain conformably by, and interdigitates with, Eyre Formation.|A basal pallid blotchy to megamottled pedolith-saprolith zone 1-2m thick in Marree Subgroup shales; grading into an overlying massive to indistinctly bedded, gravelly to pebbly lithic-rich sandstone including clasts of (an earlier) silcrete.|
22467|Mulligan Dam Regolith|70384|5|Briefly described|Map legend.|||The basal part developed as a weathering profile in Late Cretaceous shale. The upper unit displays cavernous weathering. Age: ?Paleocene (stratigraphic).|||||Basal pallid, blotchy to mottled, pedolith to saprolith zone, grading upwards through a <0.3m thick colluvial zone into massive to indistinctly bedded gravelly to pebbly sandstone, with well-rounded silcrete pebbles, yellow-grey to yellow-brown.|
23846|Muloorina Member|24175|5|Briefly described|p38|Miocene|Late Oligocene|Of the Etadunna Formation.  Persistent unit at base, of green calcareous clay and silt with thin beds of fine sand.  Geological Province: Lake Eyre Basin.||||||
23846|Muloorina Member|24321|5|Briefly described|Map legend|Miocene|Early Miocene|Parent: Etadunna Formation.||||||
23846|Muloorina Member|42746|5|Briefly described|Fig.9 P14|||Lake Eyre Basin||||||
23846|Muloorina Member|44133|5|Briefly described|p190 Fig. 10.30, 193|Early Miocene|Early Miocene|Geoloigcal Province: Lake Eyre Basin. Of the Etadunna Formation. Thickness: 15m. ||||||
23846|Muloorina Member|66131|5|Briefly described|p242 Fig.2, p243, p244 Fig.4|Miocene|Oligocene|Southern Lake Eyre region. Latest Oligocene to Early Miocene age from p.242 Fig.2 - stratigraphic correlation chart.||Of the Etadunna Formation.|||Basal fine clastic unit.|
23846|Muloorina Member|67462|5|Briefly described|Map legend.|Miocene|Miocene|Tirari Sub-basin, Lake Eyre Basin.||Unit in Etadunna Formation.||||
23846|Muloorina Member|68715|6|Mentioned|p30 Fig.5|Burdigalian|Aquitanian|Tirai and northern Callabonna sub basins, Lake Eyre Basin.||Etadunna Formation.||||07-APR-17
23846|Muloorina Member|69019|5|Briefly described|p105 Fig.25.|Miocene|Miocene|Tirari Sub-basin.||Basal unit in Etadunna Formation.||||
23846|Muloorina Member|69023|6|Mentioned|p108|Miocene|Miocene|Tirari Sub-basin, Lake Eyre Basin.||Unit in Etadunna Formation.||||
34767|Munda Group|22922|6|Mentioned|34|Early Silurian|Early Ordovician|Officer Basin.||||||
34767|Munda Group|23282|1|Redefined|p80|||"Munda Sequence" was defined by Krieg (1973), here redefined. of Officer Basin.||||||
34767|Munda Group|23479|5|Briefly described|p26|Paleozoic|Paleozoic|Geological Province: Gawler Craton.||||||07-NOV-08
34767|Munda Group|24112|5|Briefly described|p254 Fig.2|Early Silurian|Early Ordovician|Geological Province: Officer Basin.||||||24-SEP-08
34767|Munda Group|60953|5|Briefly described|Map Legend|Silurian|Silurian|Shallow marine to fluviodeltaic sandstone, siltstone and shale.||||||
34767|Munda Group|61108|5|Briefly described|map legend|Silurian|Silurian|Includes Mount Chandler Sandstone and Mintabie beds. Shallow marine to fluviodeltaic sandstone, siltstone and shale. Age: ?Silurian.||||||
34767|Munda Group|62453|5|Briefly described|p5 Fig. 3|Ordovician|Ordovician|Geological Province: Officer Basin.||||||
34767|Munda Group|64103|6|Mentioned|p400 Fig. 3|Ordovician|Ordovician|Geological Province: Officer Basin.||||||07-FEB-11
34767|Munda Group|64970|6|Mentioned|p719 Fig. 2|Silurian|Cambrian|Geological Province: Officer Basin.||||||27-MAY-09
34767|Munda Group|65313|5|Briefly described|p578, p580 Fig. 8|Ordovician|Ordovician|Officer Basin, eg. Ungoolya 1 well.|||Includes Mount Chandler Sandstone, Indulkana Shale, Blue Hills Sandstone.|Overlies Marla Group.||26-MAR-12
34767|Munda Group|65376|5|Briefly described|p9 Fig.1.2, p247 Fig.6.57.|Silurian|Ordovician||||||Marine to deltaic sediment.|
34767|Munda Group|68131|5|Briefly described|p2 Fig.1|Silurian|Ordovician|Marine to deltaic sediments.||||||
34767|Munda Group|69003|6|Mentioned|p60|Ordovician|Ordovician|E Officer Basin.||||||
34767|Munda Group|71146|5|Briefly described|p6|Llandovery|Middle Ordovician|Officer Basin.|||Includes the Mount Chandler Sandstone, Indulkana Shale and Blue Hills Sandstone.|Unconformably overlies the Table Hill Volcanics. Unconformably overlain by the Mimili Formation.|Sandstone and shale.|
34767|Munda Group|72476|6|Mentioned|p36 Fig.9|||Officer Basin. Time-temperature thermal history diagram.||||||
34767|Munda Group|72478|6|Mentioned|p8|Early Silurian|Early Ordovician|Officer Basin.|c. 495 Ma-437 Ma||Includes the Mt Chandler Sandstone, Indulkana Shale and Blue Hills Sandstone.|||
34767|Munda Group|73090|5|Briefly described|p3, p12 Fig.7|Silurian|Ordovician||||Blue Hills Sandstone, Indulkana Shale, Mount Chandler Sandstone.|||
34767|Munda Group|73099|5|Briefly described|Map legend.|Ordovician|Ordovician|Officer Basin.|||Mount Chandler Sandstone.|Overlies Marla Group.||
78691|Mundaerno Granite""|67540|5|Briefly described|p31 Tb.2|||Informally named 'Mundaerno Granite' (Leyh 1997; Fricke 2008) - now belongs to the Bimbowrie Suite. Surrounds Honeymoon Granite in TMI imagery.||Of the Bimbowrie Suite.||||12-MAR-14
78691|Mundaerno Granite""|69650|6|Mentioned|p6, p37|||An informal name, appearing in italics. Often surrounds Honeymoon Granite.||Unit in Bimbowrie Suite.||||
24409|Mundallio Subgroup|22772|5|Briefly described|Table13.1|Cryogenian|Cryogenian|||||||
24409|Mundallio Subgroup|22857|5|Briefly described|Tb. 13.1 (insert p70-71)|Torrensian|Torrensian|Of the Burra Group.||||||
24409|Mundallio Subgroup|22869|5|Briefly described|P37, P38, Table2|||||||||
24409|Mundallio Subgroup|22889|4|Described|p34|Adelaidean|Adelaidean|The Mundallio Subgroup is redefined to exclude the Woolshed Flat Shale from the unit, see p 34 for details.||||||
24409|Mundallio Subgroup|23054|6|Mentioned|p11|||||||||
24409|Mundallio Subgroup|24175|6|Mentioned|p11|Neoproterozoic|Neoproterozoic|Term used by Uppill (1979) to refer to Woolshed Flat Shale and Skillogalee Dolomite within the Burra Group.||||||
24409|Mundallio Subgroup|24321|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Burra Group.||||||14-MAY-07
24409|Mundallio Subgroup|24546|5|Briefly described|p2 - 3 Fig.2|Neoproterozoic|Neoproterozoic|Of Burra Group. Overlain by Undalya Quartzite. Geological Province: Adelaide Fold Belt.||||||16-JAN-08
24409|Mundallio Subgroup|38926|4|Described|p26|||||||||
24409|Mundallio Subgroup|39320|6|Mentioned|p375|||||||||
24409|Mundallio Subgroup|41401|6|Mentioned|Table 4|||||||||
24409|Mundallio Subgroup|41404|4|Described|p98|||Mention p105.||||||14-MAY-07
24409|Mundallio Subgroup|41526|6|Mentioned|p3|||||||||
24409|Mundallio Subgroup|42098|6|Mentioned|Table 2 P54|||||||||
24409|Mundallio Subgroup|42222|4|Described|p13|||||||||
24409|Mundallio Subgroup|42236|4|Described|p107|||See also Fig.2||||||
24409|Mundallio Subgroup|42238|5|Briefly described|p72|||||||||
24409|Mundallio Subgroup|43052|4|Described|p179|||Of the Burra Group.||||||14-MAY-07
24409|Mundallio Subgroup|60718|5|Briefly described|p49 Fig. 2|Adelaidean|Adelaidean|Geological Province: Adelaide Geosyncline.||Of Burra Group.|Includes Skillogalee Dolomite.|||15-APR-11
24409|Mundallio Subgroup|60959|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Of the Burra Group.||||||
24409|Mundallio Subgroup|61238|5|Briefly described|p44 Fig. 1|Neoproterozoic|Neoproterozoic|Of the Burra Group.||||||
24409|Mundallio Subgroup|62592|5|Briefly described|p50 Table 5.1, pp57-58.|Torrensian|Torrensian|Adelaide Geosyncline. Produces strong seismic reflections.||Unit in Burra Group.|Includes Skillogalee Dolomite.|Overlies Emeroo Subgroup. Is overlain by Bungarider Subgroup.|Dolomite, magnesite, sandstone, siltstone.|
24409|Mundallio Subgroup|62724|5|Briefly described|p17 Fig. 4|Torrensian|Torrensian|Of the Burra Group.||||||07-FEB-11
24409|Mundallio Subgroup|63489|5|Briefly described|Map legend|Adelaidean|Adelaidean|Includes Skillogalee Dolomite.||||||10-SEP-07
24409|Mundallio Subgroup|66884|5|Briefly described|p36, p41 Fig.3|||||Burra Group|Skillogalee Dolomite|||
24409|Mundallio Subgroup|67870|5|Briefly described|p9|Neoproterozoic|Neoproterozoic|Adelaide Rift System.||Burra Group.|Skillogalee Formation.|||
24409|Mundallio Subgroup|69019|6|Mentioned|p39-41.|Neoproterozoic|Neoproterozoic|Of Uppill (1979); revision by Preiss and Cowley (1999) excludes Woolshed Flat Shale and other sandstone units to the south.||||||
24409|Mundallio Subgroup|70384|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Adelaide Geosyncline.||Burra Group.|Skillogalee Dolomite.|Overlies Emeroo Subgroup. Is overlain by Bungarider Subgroup.||
24409|Mundallio Subgroup|70405|6|Mentioned|p50, p51 table 4|Neoproterozoic|Neoproterozoic||790 Ma||Includes Skilloglaee Dolomite||Carbonate rocks.|
24409|Mundallio Subgroup|70819|6|Mentioned|p11, 13|Neoproterozoic|Neoproterozoic|Clare Valley.||Burra Group.|Skillogalee Dolomite, Marola Sandstone.|Overlies Emeroo Subgroup. Is overlain disconformably by Bungarider Subgroup.||
24409|Mundallio Subgroup|73188|5|Briefly described|p316, p326|Neoproterozoic|Neoproterozoic|Mount Lofty Ranges.||Burra Group|Montacute Dolomite, Castambul Formation|||
24409|Mundallio Subgroup|74367|5|Briefly described|p7 Fig.6, p8, p18|Tonian|Tonian|||Burra Group|Skillogalee Dolomite, Kooringa Member|||
78851|Mundawertina Formation|66464|6|Mentioned|p176-177 Fig.10|||Presented as Mundawertina Fm in figure caption. Presumably named after Mundawertina Well. Said to overlie dolostone of Nuccaleena Formation. Limestone. Also appears as Mundawertina Mb on p178, but with no parent identified.|||||Limestone.|15-MAY-14
79316|Mundy Dam Microgranite|71416|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|SHRIMP U-Pb zircon magmatic crystallisation age.|c.1140 Ma (Jagodzinski et al., in prep.).||||Microgranite to micromonzonite, biotite, inequigranular to locally porphyritic, massive to foliated.|
25309|Munetta Sand|38290|5|Briefly described|p59|||||||||
33688|Munjeela Suite|65772|5|Briefly described|p228, p229 Fig.2|Statherian|Statherian|Consists of a small number of muscovite-garnet-bearing plutons aged c.1590-1580 Ma (Payne, 2008). Also referred to as Munjeela Granite in Fig. 2||||||08-SEP-14
33688|Munjeela Suite|66519|2|Defined|pp31-34.|Mesoproterozoic|Mesoproterozoic|S-type granites exposed at Munjeela Rockhole (inf. n.), Point Bell and Point Sinclair. Coeval with Gawler Range Volcanics-Hiltaba Suite magmatic event. Locally deformed and sheared. Local enclaves of deformed metasediments. Isolated outcrops.|c.1590-1575 Ma (Payne 2008).||Includes Point James Granite and Point Sinclair Granite.||Leucogranites: coarse-grained quartz, K-feldspar and plagioclase; muscovite and biotite +/- garnet occurring interstitially; tourmaline as occasional accessory. Limited mineralisation potential.|
33688|Munjeela Suite|67900|5|Briefly described|p22, 32|Mesoproterozoic|Mesoproterozoic|Western Gawler Craton.|c.1585 Ma.||||S-type intrusives formed by partial melting of a metasedimentary protolith.|
33688|Munjeela Suite|70337|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic||1590-1575 Ma (U-Pb).||||Leucogranite, quartz + K-feldspar + plagioclase + muscovite + biotite +/- garnet, coarse-grained, S-type, peraluminous. Deformation varies from none to mylonitic.|
33688|Munjeela Suite|70659|5|Briefly described|p2|Mesoproterozoic|Mesoproterozoic|Associated with Gawler Range Volcanics.|c.1585 Ma||||S-type.|
33688|Munjeela Suite|70778|6|Mentioned|p24-p25|||Nuyts Domain, Gawler Craton. See also Munjeela Granite in Fig. 18, p25, described as pne of the largest plutons in the Munjeela Suite.||||||05-SEP-19
33688|Munjeela Suite|70816|5|Briefly described|p4|||Gawler Ranges region.|~1585 Ma||||S-type granites.|
33688|Munjeela Suite|71129|6|Mentioned|p47|Calymmian|Calymmian|Geological Province: Gawler Craton. S-type magmatism associated with Gawler Range Volcanics and Hiltaba Suite.|c. 1585 Ma|||||
33688|Munjeela Suite|71317|5|Briefly described|p20, p175|Calymmian|Calymmian||c. 1590-1575 Ma||Includes the Point James Granite.|||
33688|Munjeela Suite|72090|5|Briefly described|p9|||Gawler Craton.|||||S-type granitic rocks.|
33688|Munjeela Suite|73030|6|Mentioned|p2150|||S-type granites. Constitutes the intrusive equivalent of the Gawler Range Volcanics.||||Equivalent to Gawler Range Volcanics and Hiltaba Suite.||
33688|Munjeela Suite|73233|6|Mentioned|p26, p27 Fig.1|Mesoproterozoic|Mesoproterozoic|Gawler Craton, Nyuts Domain.|||||Igneous Intrusions.|
23851|Munjena Formation|22587|6|Mentioned|p79 Fig.7|Late Oligocene|Late Oligocene|||||||
23851|Munjena Formation|22613|5|Briefly described|p24|||||||||
23851|Munjena Formation|22614|5|Briefly described|map|Tertiary|Tertiary|||||||
23851|Munjena Formation|40912|6|Mentioned|Map legend|Miocene|Oligocene|Oligocene-Miocene||||||
23851|Munjena Formation|42465|6|Mentioned|Map Legend|||||||||
23851|Munjena Formation|42469|5|Briefly described|p38|||||||||
23851|Munjena Formation|42816|4|Described|p24|||||||||
23851|Munjena 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
23851|Munjena Formation|43258|5|Briefly described|Map Legend|Pliocene|Paleocene|||||||
23851|Munjena Formation|43298|6|Mentioned|Map Legend|Pleistocene|Tertiary|||||||
23851|Munjena Formation|44133|5|Briefly described|p185, 180 Fig. 10.22|Quaternary|Pliocene|Geological Province: Eucla Basin. Thickness: 3m. ||||||
23851|Munjena Formation|44695|5|Briefly described|Map Legend||Tertiary|||||||
23851|Munjena Formation|60953|5|Briefly described|Map Legend|Miocene|Eocene|Alluvial, colluvial and residual clastics, commonly silicified or ferruginised.||||||27-APR-05
23851|Munjena 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: Eucla Basin palaeodrainage.||||||02-JUN-05
23851|Munjena Formation|61155|5|Briefly described|p17|Middle Miocene|Early Miocene|Geological region: Oodnadatta area.||||||
23851|Munjena Formation|64646|6|Mentioned|p23 Fig. 3|Pleistocene|Oligocene|Geological Province: Gawler Craton.||||||08-FEB-10
23851|Munjena Formation|67462|5|Briefly described|Map legend.|||Eucla Basin. Shown as two separate units, one Oligocene, the other Pliocene, in NW Gawler part of Eucla Basin (ie NE Eucla)||||||15-JAN-15
23851|Munjena Formation|68128|5|Briefly described|p43, p64, p71, p77|Pliocene|Eocene|Gawler Craton.|||||Conglomeratic sand, clayey sand, and breccia. Poorly sorted.|01-FEB-23
23851|Munjena Formation|68715|6|Mentioned|p30 Fig.5|Chattian|Rupelian|NW Gawler Craton, Eucla Basin.||||||
23851|Munjena Formation|69598|6|Mentioned|p9|Late Oligocene|Late Oligocene|||||||
34807|Munta Limestone Member|22922|5|Briefly described|33|Neoproterozoic|Neoproterozoic|Age: Marinoan. Member of Punkerri Sandstone?||||||
34807|Munta Limestone Member|23282|2|Defined|p66||Neoproterozoic|Informally defined as Munta Limestone by Sukanata (1993), now defined as member of Narana Formation. Age: Precambrian, Neoproterozoic, late Marinoan Epoch. of Officer Basin.||||||
34807|Munta Limestone Member|24112|5|Briefly described|p254 Fig.2|Neoproterozoic|Neoproterozoic|Of the Ungoolya Group. Geological Province: Officer Basin||||||
34807|Munta Limestone Member|61732|4|Described|p58 Fig. 22, p66|Ediacaran|Ediacaran|Of the Narana Fm (Ungoolya Gp). Grey to greenish-grey massive and laminated micritic mudstone and marl that are rhythmically interbedded. Conformably overlain by Mena Mudst Mbr. Thick: 45m. Geol Prov: Officer Basin. See also p145 Fig. 51.||||||07-FEB-11
34807|Munta Limestone Member|72478|6|Mentioned|p8|Marinoan|Marinoan|Officer Basin.|c. 570 Ma|Narana Formation||Underlies the Mena Mudstone Member.||24-MAR-21
34807|Munta Limestone Member|73099|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Officer Basin.||Narana Formation.||Is overlain by Mena Mudstone Member.|Grey micritic limestone and calcareous mudstone, laminated to thin-bedded in part.|
22479|Munyarai Formation|22746|4|Described|Fig.3 p515, p521|Neoproterozoic III|Neoproterozoic III|||||||
22479|Munyarai Formation|22922|6|Mentioned|34|||Parent Ungoolya Group||||||
22479|Munyarai Formation|23282|2|Defined|p64||Neoproterozoic|of Zang (1995). Age: Precambrian, Neoproterozoic, mid-late Marinoan. of Ungoolya Group, Officer Basin.||||||
22479|Munyarai Formation|23524|5|Briefly described|p221 Fig. 3|Neoproterozoic|Neoproterozoic|||||||
22479|Munyarai Formation|24112|5|Briefly described|p254 Fig.2|Neoproterozoic|Neoproterozoic|Of the Ungoolya Group. Geological Province: Officer Basin||||||
22479|Munyarai Formation|43743|6|Mentioned|Fig.2,p33||Neoproterozoic|||||||
22479|Munyarai Formation|61732|3|Fully described|p12 Tb. 3, p65|Ediacaran|Ediacaran|Of Ungoolya Group. Conformably overlies Tanana Fm; underlies Narana Fm. Occurs in the Munyarai Trough. Max. thickness: almost 450m. Geol.Prov: Officer Basin. See also p58 Fig. 22, p145 Fig. 51.||||||07-FEB-11
22479|Munyarai Formation|63397|2|Defined|p31-32|Neoproterozoic III|Neoproterozoic III|Of the Ungoolya Group. Type section in text. Grey to dark-grey calcareous siltstone with thin limestone interbeds. Thickness: 448m. Conformably overlies the Tanana Formation. Unconformably overlain by Narana Formation.||||||
22479|Munyarai Formation|64794|6|Mentioned|p244, p274|Ediacaran|Ediacaran|||Ungoolya Group||||
22479|Munyarai Formation|64797|6|Mentioned|p153 Fig.2|Ediacaran|Ediacaran|Officer Basin. Lithology/rank not shown on diagram.||||||
22479|Munyarai Formation|65892|6|Mentioned|p35.|Late Neoproterozoic|Late Neoproterozoic|Mis-spelt as Munyerai. Contains new, spinose acritarchs.||||||
22479|Munyarai Formation|66569|5|Briefly described|p860, p861 fig.2,|Ediacaran|Ediacaran|Correlated with Wonoka Formation; of Ungoolya Group; unconformably underlies Narana Formation; unconformably overlies Tanana Formation.||||||
22479|Munyarai Formation|68269|6|Mentioned|p674|Ediacaran|Ediacaran|Officer Basin.||Ungoolya Group||Unconformably underlain by Tanana Formation. Unconformably overlain by Narana Formation.|Mudstone dominated.|
22479|Munyarai Formation|72478|6|Mentioned|p8|Marinoan|Marinoan|Officer Basin.|c. 575 Ma|Ungoolya Group||Overlies the Tanana Formation. Unconformably overlain by the Punkerri Sandstone.||24-MAR-21
31511|Murbko Marl Member|23226|2|Defined|p899||Balcombian|Age: Foraminifers indicate a Balcombian age, supported by strat position. May intertongue with laterally equivalent Overland Corner Clay Member. May be broken up informally into upper and lower. Of Cadell Formation.||||||
31511|Murbko Marl Member|64237|5|Briefly described|p19 Fig. 2b|Middle Miocene|Middle Miocene|Of Cadell Formation (Morgan Subgroup, Murray Group); introduced as member of the Morgan Group (Murray Supergroup) by Lukasik and James (1998) and retained as part of Morgan Subgroup when Murray Group was reinstated.. Geological Province: Murray Basin.||||||29-JUL-08
26316|Murnaroo Formation|22613|4|Described|p16|Neoproterozoic|Neoproterozoic|Officer Basin||||||
26316|Murnaroo Formation|22649|6|Mentioned|p 151|||Province - Officer basin.||||||
26316|Murnaroo Formation|22922|5|Briefly described|34|||Parent Lake Maurice Group||||||
26316|Murnaroo Formation|23282|2|Defined|p58||Neoproterozoic|Age: Precambrian, Neoproterozoic, early Marinoan Epoch. Of Gatehouse et al (1986). Unit is equivalent to part of the Wright Hill beds of Major (1973). Of Lake Maurice Group, Officer Basin.||||||12-JAN-16
26316|Murnaroo Formation|23287|6|Mentioned|Fig.2,4|||Age: Lower Ediacaran. of Eastern Officer Basin.||||||11-SEP-14
26316|Murnaroo Formation|23524|5|Briefly described|p221 Fig. 3|Neoproterozoic|Neoproterozoic|||||||
26316|Murnaroo Formation|24112|5|Briefly described|p254 Fig.2, p257 Tb.1|Neoproterozoic|Neoproterozoic|Of the Lake Maurice Group. Age: 640-600Ma. Geological Province: Officer Basin||||||
26316|Murnaroo Formation|40432|2|Defined|p17|Middle Cambrian|Early Cambrian|Late Early - early Middle Cambrian||||||04-SEP-14
26316|Murnaroo Formation|40912|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
26316|Murnaroo Formation|40945|3|Fully described|p14|||||||||
26316|Murnaroo Formation|41833|6|Mentioned|p586|||||||||
26316|Murnaroo Formation|42095|5|Briefly described|Fig.3 P31|||||||||
26316|Murnaroo Formation|42096|6|Mentioned|p36|||||||||
26316|Murnaroo Formation|42356|5|Briefly described|Fig.15 P119|Cambrian|Neoproterozoic|See also Microfiche 7 p15, Fig.4, Fig.9, 10, 12, 13.||||||
26316|Murnaroo Formation|42816|3|Fully described|p13|||||||||
26316|Murnaroo Formation|43650|6|Mentioned|Fig.2,p444|||||||||
26316|Murnaroo Formation|43657|6|Mentioned|Fig.3,p4||Neoproterozoic|||||||
26316|Murnaroo Formation|43690|6|Mentioned|Fig.2,p157||Neoproterozoic|||||||
26316|Murnaroo Formation|43732|5|Briefly described|p3-4|||||||||
26316|Murnaroo Formation|43743|6|Mentioned|Fig.2,p33||Neoproterozoic|||||||
26316|Murnaroo Formation|44109|5|Briefly described|p22 Fig. 19|Neoproterozoic|Neoproterozoic|Geological Province: central Officer Basin.||||||
26316|Murnaroo Formation|50127|6|Mentioned|p48 Fig.2|||Geological Province: Officer Basin||||||
26316|Murnaroo Formation|60565|5|Briefly described|p20 Fig. 3b|||Overlain by the Rodda beds.||||||
26316|Murnaroo Formation|61732|3|Fully described|p5 Tb. 1, p59-60|Cryogenian|Cryogenian|Of Lake Maurice Group. Overlies Meramangye Fm, Tarlina Sst.or Alinya Fm; conformably overlain by Dey Dey Mudst., or unconformably by Relief Sst. Geol.Prov: Officer Basin. See also p58 Fig. 22, p127, p145 Fig. 51.||||||07-FEB-11
26316|Murnaroo Formation|62570|5|Briefly described|p580 Fig. 2|Middle Cambrian|Middle Cambrian|Of the Marla Group. Geological Province: Officer Basin.||||||10-AUG-07
26316|Murnaroo Formation|63397|6|Mentioned|5, 10|Neoproterozoic III|Neoproterozoic III|Of the Maurice Group. Thickness 390m.||||||23-JUL-07
26316|Murnaroo Formation|63811|6|Mentioned|p501 Fig 2|||||Of Lake Maurice Group.||||28-MAR-12
26316|Murnaroo Formation|64794|4|Described|p238 fig 2, p241 Tb.1, p242 fig 3 |Ediacaran|Ediacaran|See also p244-6, p255, p258, p273. Thickness over 105 m.||Lake Maurice Group||Overlain by Dey Dey Mudstone (conformably).|Very coarse quartzo-feldspathic sandstone, fine-pebble feldspathic conglomerate, and red and green shale interbeds; underlain by 83m of fine to medium quartzose cross-bedded sandstones, rare cosets of laminated fine sandstone and red siltstone.|
26316|Murnaroo Formation|65376|6|Mentioned|p247 Fig.6.57.|Neoproterozoic|Neoproterozoic|||||||
26316|Murnaroo Formation|67912|5|Briefly described|p13-14|Ediacaran|Ediacaran|Eastern Officer Basin. Subsurface; penetrated by the Lake Maurice West 1 drillhole.||||Is overlain by Ungoolya Group.||
26316|Murnaroo Formation|69648|4|Described|p17-19, map legend|Neoproterozoic|Neoproterozoic|Regression. Age: Marinoan. Continuously shallowing-upwards into shoreface and estuarine-fluvial sediments. Probable equivalents of this unit have been interpreted from drillhole logs.||Lake Maurice Group||Conformably to unconformably overlies Meramangye Formation, Tarlina Sandstone or Alinya Formation.|Very fine to coarse feldspathic quartz sandstone, locally pyritic, calcareous or dolomitic to micaceous or glauconitic; interbedded shale and siltstone, minor (micritic) dolostone, fine-grained quartz sandstone, conglomerate, and dolomitic shale.|17-FEB-15
26316|Murnaroo Formation|70336|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic||||||Pale grey-green to green sandstone, fine- to coarse-grained, with shale interbeds.|
26316|Murnaroo Formation|72478|6|Mentioned|p8|Marinoan|Marinoan|Officer Basin.|c. 640-600 Ma|Lake Maurice Group||Overlies the Meramangye Formation and the Tarlina Sandstone.||24-MAR-21
26316|Murnaroo Formation|73090|5|Briefly described|p12 Fig.7, Appendix|Cambrian|Cambrian||||||Pale grey-green to green sandstone, fine- to coarse-grained, with shale interbeds.|
26316|Murnaroo Formation|73099|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Officer Basin.||Lake Maurice Group.||Overlies Meramangye Formation. Is overlain by Dey Dey Mudstone.|Reddish grey, brown and grey, very fine to very coarse, micaceous quartz and feldspathic quartz sandstone, with interbeds of claystone, siltstone and conglomerate; heavy mineral banding.|
26316|Murnaroo Formation|73108|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic||||||Pale grey-green to green sandstone, fine to coarse-grained, with shale interbeds.|
26316|Murnaroo Formation|73392|6|Mentioned|p3||||||||Sampled from core of Giles 1, Munta 1 wells.|
81157|Murninnie mylonite|71413|6|Mentioned|p32 Fig 2|||Geological province: Gawler Craton. ||||||
29846|Mustering Paddock Formation|22884|2|Defined|p40 Fig. 1, p46||Paleoproterozoic|Of the Sundown Group. Overlain by Mount Howden Formation; underlain by Weekeroo Formation. Max. thickness is 300m. Predominantly psammitic and psammopelitic metasediments, siliciclastic, thin to thick bedded+ common sed'y structures, and local calc-silica||||||26-MAR-09
29846|Mustering Paddock Formation|23347|6|Mentioned|p54|||Of Laing (1996a). Written as "Mustering Paddock Formation".  Possibly a synonym of Saltbush Subgroup.||||||
29846|Mustering Paddock Formation|62641|6|Mentioned|p286 Fig.9.|||Age from a rhyolite unit.|c.1713 Ma (Ozchron).|||||
29846|Mustering Paddock Formation|63102|6|Mentioned|p34|||Geological province: Broken Hill Domain, Curnamona Province. Nomenclature of Laing (1996b). Now considered to equate to Peryhumuck Formation.||||||
29846|Mustering Paddock Formation|70657|6|Mentioned|p41|||Laing (1996)'s interpretation is incorrect; this is actually the Peryhumuck Formation (Curnamona Group) so is older than the Sundown Group.||||||
70229|Mutooroo Gneiss|62728|2|Defined|p24|Mesoproterozoic|Paleoproterozoic|Part of the Silver City Suite. Formerly the informal Mutooroo gneiss. Well-foliated, biotite, adamellitic to granodioritic, augen gneiss. S-type. Age samples have given 1709+/-6Ma and 1696+/-17Ma. Geol Prov: Broken Hill Domain/Curnamona Province.||||||07-FEB-11
23856|Myola Volcanics|22629|5|Briefly described|p152, figs2,4|Statherian|Statherian|U-Pb age of 1791+/-4 Ma||||||
23856|Myola Volcanics|23054|6|Mentioned|p9||Statherian|Max Age: 1791 (+/-) 4 Ma.||||||
23856|Myola Volcanics|23481|5|Briefly described|p19 Fig 1|||Geological Province: Gawler Craton.||||||
23856|Myola Volcanics|23719|4|Described|p16|Statherian|Statherian|See also page 14 table 1, page 15 table 2. Age: 1791+/-4 Ma (U-Pb zircon). Overlain by Broadview Schist. Underlain by Hutchinson Group. Geological Province: Gawler Craton.||||||18-JAN-07
23856|Myola Volcanics|23805|5|Briefly described|p4 Fig. 1|Paleoproterozoic|Paleoproterozoic|Geological Province: Gawler Craton.||||||07-NOV-08
23856|Myola Volcanics|24197|5|Briefly described|p75 Tb. 8.1, p130|Paleoproterozoic|Paleoproterozoic|Age: 1791Ma. Geological province: Gawler Craton.||||||07-FEB-11
23856|Myola Volcanics|24505|5|Briefly described|p5 Fig. 1|||Geological Province: Gawler Craton.||||||
23856|Myola Volcanics|24526|6|Mentioned|p99|Paleoproterozoic|Paleoproterozoic|Age: 1790Ma.||||||07-NOV-08
23856|Myola Volcanics|37811|6|Mentioned|Fig.2|||||||||
23856|Myola Volcanics|39349|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
23856|Myola Volcanics|39802|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
23856|Myola Volcanics|39911|6|Mentioned|p5|||||||||
23856|Myola Volcanics|40448|4|Described|p32|||||||||
23856|Myola Volcanics|40644|4|Described|p120 Fig. 2, p129-130|Paleoproterozoic|Paleoproterozoic|Multiple deformed rhyolites, rhyodacites.||||||07-NOV-08
23856|Myola Volcanics|41239|6|Mentioned|p95|||||||||
23856|Myola Volcanics|41325|6|Mentioned|p18|||||||||
23856|Myola Volcanics|41402|6|Mentioned|p35|||||||||
23856|Myola Volcanics|41493|6|Mentioned|Table 1|||||||||
23856|Myola Volcanics|41609|6|Mentioned|Fig.1|||||||||
23856|Myola Volcanics|41667|4|Described|p75|||||||||
23856|Myola Volcanics|41972|4|Described|p373|||||||||
23856|Myola Volcanics|42546|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
23856|Myola Volcanics|42736|5|Briefly described|map legend|Paleoproterozoic||||||||07-NOV-08
23856|Myola Volcanics|42934|5|Briefly described|p520|||||||||
23856|Myola Volcanics|43052|4|Described|p62|||Age of 1791+/-4 Ma.||||||18-JAN-07
23856|Myola Volcanics|43053|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Metarhyolite, metarhyodacite.||||||07-NOV-08
23856|Myola Volcanics|43141|6|Mentioned|p63,Fig.1||Proterozoic|||||||
23856|Myola Volcanics|43258|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
23856|Myola Volcanics|43298|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
23856|Myola Volcanics|43561|6|Mentioned|p1438|||||||||
23856|Myola Volcanics|43583|6|Mentioned|p2163|||Age: 1791+/-4 Ma||||||
23856|Myola Volcanics|50605|5|Briefly described|p(iii), 3.3, 11.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Gawler Craton & Curnamona Province. Age: 1791 +/- 4Ma.||||||07-NOV-08
23856|Myola Volcanics|60515|6|Mentioned|p116 Fig.1 |||||||||
23856|Myola Volcanics|60953|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Age: 1791Ma. Porphyritic rhyolite to rhyodacite.||||||07-NOV-08
23856|Myola Volcanics|60954|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Geological Province: Gawler Craton.||||||07-NOV-08
23856|Myola Volcanics|61108|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|Porphyritic rhyolite to rhyodacite. Age: 1791 Ma.||||||07-NOV-08
23856|Myola Volcanics|61262|5|Briefly described|p455 Fig. 11|Paleoproterozoic|Paleoproterozoic|Age: <1800Ma. Geological Province: eastern Gawler Craton.||||||07-NOV-08
23856|Myola Volcanics|61307|5|Briefly described|p36 Fig. 17|Paleoproterozoic|Paleoproterozoic|Geological Province: Gawler Craton. See also p39 Fig. 19.||||||07-NOV-08
23856|Myola Volcanics|61522|5|Briefly described|p5 Fig.1|||Geological Province: Gawler Craton.||||||
23856|Myola Volcanics|61936|6|Mentioned|p203|||Geological Province: Gawler Craton. ||||||
23856|Myola Volcanics|62536|6|Mentioned|p658|||Gawler Craton.||||||
23856|Myola Volcanics|62893|6|Mentioned|p12|Palaeoproterozoic|Palaeoproterozoic|Gawler Craton.||||||
23856|Myola Volcanics|63866|5|Briefly described|p5, p9, p20|Statherian|Statherian|Spencer Domain, Gawler Craton. Shortened to Myola Volc on p9.|1791 +/- 4 Ma Ma (Fanning et al., 1988)|||||
23856|Myola Volcanics|64130|5|Briefly described|p1378 Fig.1, p1380 Fig.2, p1381  |Paleoproterozoic|Paleoproterozoic|Bimodal volcanics: marks post-Donington Suite rifting along eastern margin of the Gawler Craton.|1791 +/- 4 Ma (Fanning et al., 1988).||||Bimodal volcanics.|
23856|Myola Volcanics|64313|5|Briefly described|p450 Fig. 1|Paleoproterozoic|Paleoproterozoic|Age: 1791+/-4Ma (U-Pb zircon). Geological province: Gawler Craton.  See also p451 Fig.2b.||||||09-FEB-10
23856|Myola Volcanics|64725|6|Mentioned|p58 Fig.2. |||Gawler Craton.||||||
23856|Myola Volcanics|64744|6|Mentioned|p367.|Statherian|Statherian||1790 Ma.|||||
23856|Myola Volcanics|65221|5|Briefly described|p26|Palaeoproterozoic|Palaeoproterozoic|Volcano-sedimentary sequences overlying the Hutchison Group, 1790Ma. Cleve Domain.||||||14-MAR-10
23856|Myola Volcanics|65376|6|Mentioned|p8 Fig.1.1, p109, p231.|Paleoproterozoic|Paleoproterozoic|This unit may be the source of detrital zircons of this age in Mona Volcanics Member. Has geochemical similarities with felsic units of Tidnamurkuna Volcanics.|c.1790 Ma.||||Felsic volcanic rocks.|02-APR-14
23856|Myola Volcanics|65390|5|Briefly described|p18, p23 Fig.3|Statherian|Statherian|Spencer Domain, Gawler Craton. Underlies Broadview Schist. Age of c. 1790 Ma given.||||||
23856|Myola Volcanics|65772|6|Mentioned|p229 Fig.2|Statherian|Statherian|c.1.78-1.74 Ga.||||||
23856|Myola Volcanics|65915|5|Briefly described|p5-6|Statherian|Statherian|Sedimentary and volcanic rocks deposited between ~1790-1740 Ma east of Kalinjala Mylonite Zone.||||||
23856|Myola Volcanics|65922|5|Briefly described|p13 Fig.4, p29 Fig.6|Statherian|Statherian|Gawler Craton.||||||
23856|Myola Volcanics|66302|4|Described|p4 Fig.3, p28, p33, p34, p63|Statherian|Statherian|Spencer Domain, Gawler Craton. U-Pb crystallisation ages. Ages derived from Fanning et al. (1988) and Fraser and Neumann (2010) respectively. |1791 +/- 4 Ma  to 1792 +/- 5 Ma |||Intruded by the Wertigo Granite. Overlain by the Broadview Schist.|Interbanded porphyritic rhyolite and rhyodacite, fine-grained felsic and hornblende-bearing gneisses and amphibolite.|
23856|Myola Volcanics|66882|5|Briefly described|p102, p109 Tb.1, p114 Fig.11, p117-120|Statherian|Statherian|Northern Eyre Peninsula. Isotope data. Possible source of c.1790 Ma zircons in Cleve Group.|1790 Ma (Sm-Nd and zircon Lu-Hf)|||||
23856|Myola Volcanics|67058|5|Briefly described|p476.|Paleoproterozoic|Paleoproterozoic||1791 +/- 4 Ma (Fanning et al. 1998).|||||
23856|Myola Volcanics|67323|5|Briefly described|Eastern Australia Time-Space Plot; p31|||Gawler Craton.|1792 +/- 5 Ma.|||||
23856|Myola Volcanics|67536|5|Briefly described|Map Legend|Statherian|Statherian|Gawler Craton.|1791 +/- 4 Ma||||Rhyolite to rhyodacite.|
23856|Myola Volcanics|67581|6|Mentioned|p45|||Gawler Craton. Pre-Kimban (1790-1740 Ma) Orogeny.||||||
23856|Myola Volcanics|67721|5|Briefly described|p34, p35 Fig.6|Statherian|Statherian||c. 1790 Ma|||||
23856|Myola Volcanics|67900|6|Mentioned|p20|Paleoproterozoic|Paleoproterozoic|Fanning et al. (1988). Eastern Gawler Craton.|c.1790 Ma.|||||
23856|Myola Volcanics|68131|5|Briefly described|p2 Fig.1|Paleoproterozoic|Paleoproterozoic|Mapped with Broadview Schist as a single unit.|||||Included in a polygon of schist, quartzite, amphibolite and felsic volcanic rocks.|
23856|Myola Volcanics|68158|5|Briefly described|p1-2, p4-8, p13-16, p19|||Parker et al. (1988). The type locality is N of Myola homestead. Also gives ID-TIMS U-Pb zircon age of 1791 +/- 4 Ma (Fanning et al., 1988). Sm-Nd values; age determination problem discussed.|1792 +/- 5 Ma (SHRIMP U-Pb zircon).||||Greenschist facies quartz trachyte, hornblende trachyte, feldspathic metasandstone.|
23856|Myola Volcanics|68208|6|Mentioned|p32 Fig.3, p33, p34 Fig.5, p35|Paleoproterozoic|Paleoproterozoic|Grouped with Broadview Schist and described as terrestrial volcanics and sediments. Shows strong fabric from Kimban Orogeny.|C. 1790|||||
23856|Myola Volcanics|69048|6|Mentioned|p3|||Eyre Peninsula / Yorke Peninsula.|c.1775-1750 Ma.|||||
23856|Myola Volcanics|69649|6|Mentioned|p6 Fig.4|||||||||
23856|Myola Volcanics|69666|6|Mentioned|p27 Fig.3|Paleoproterozoic|Paleoproterozoic|||||||
23856|Myola Volcanics|70027|5|Briefly described|p56-57,71|Paleoproterozoic|Paleoproterozoic|Geological province: Gawler Craton. Rhyolitic assemblage on the Eyre Peninsula. Possible source of ca. 1790-1750 Ma zircons associated with the Warramboo magnetite gneiss.|ca. 1790 Ma||||Rhyolitic volcanics.|17-JUL-19
23856|Myola Volcanics|70334|5|Briefly described|p74|Statherian|Statherian|Geological province: Gawler Craton. |c. 1790 Ma|||Overlain by Moonabie Formation.||
23856|Myola Volcanics|70405|6|Mentioned|p12 figure 4|Paleoproterozoic|Paleoproterozoic||1790 Ma|||||
23856|Myola Volcanics|70659|6|Mentioned|p4, p10|Palaeoproterozoic|Palaeoproterozoic|Kimban Orogeny (1730-1690 Ma) tectonic fabrics were folded by (~1620-1570 Ma) Kararan Orogeny.||||||
23856|Myola Volcanics|70721|6|Mentioned|p63-p64, p66, p73|Paleoproterozoic|Paleoproterozoic||c. 1795 Ma|||Faulted against the Cooyerdoo Granite.|Felsic and mafic volcanics.|
23856|Myola Volcanics|70816|5|Briefly described|p3-4|Statherian|Statherian|Gawler Ranges region. Underwent LT metamorphism during 1730-1690 Ma Kimban Orogeny.|~1790 Ma|||||
23856|Myola Volcanics|70948|5|Briefly described|p974-975|Statherian|Statherian|Geological province: Gawler Craton.|ca. 1790 Ma|||In faulted contact with Cooyerdoo Granite. Underwent LT metamorphism during 1730-1690 Ma Kimban Orogeny.||
23856|Myola Volcanics|71037|5|Briefly described|p21 Fig.1, p24|Paleoproterozoic|Paleoproterozoic|Described as deposited in a marine shoreface environment.|c. 1795 Ma|||Coeval with Broadview Schist. Shown as younger than Hutchison Group and older than Wertigo Granite.|Felsic volcanics.|
23856|Myola Volcanics|71129|6|Mentioned|p14,17-18,23,204|Statherian|Statherian|Geological Province: Spencer Domain, Gawler Craton.|c. 1795 Ma|||Contemporaneous with Hutchison Group.||
23856|Myola Volcanics|71235|6|Mentioned|p3, p9, p13|Palaeoproterozoic|Palaeoproterozoic||c. 1790 Ma (Fanning et al., 1988)|||||
23856|Myola Volcanics|71317|6|Mentioned|p15-p16|Palaeoproterozoic|Palaeoproterozoic|Gawler Craton.|c. 1790 Ma|||||
23856|Myola Volcanics|71341|6|Mentioned|p194, p196|||Broadly geochemically similar to the McGregor Volcanics, Cleve Group, Price Metasediments, Moonabie Formation and the Wallaroo Group. |ca. 1790 Ma (Szpunar and Fraser, 2010)|||||
23856|Myola Volcanics|71348|5|Briefly described|p201,212|Statherian|Statherian|Geological province: Gawler Craton. Coeval with deposition of Broadview Schist sedimentary rocks. Formed in a back-arc setting consistent with mafic and bimodal magmatism.|c. 1790 Ma|||||
23856|Myola Volcanics|71413|6|Mentioned|p32 Fig 2|||Geological province: Gawler Craton. ||||||
23856|Myola Volcanics|71534|6|Mentioned|p296|Statherian|Statherian|Geological province: Gawler Craton.||||||
23856|Myola Volcanics|71559|6|Mentioned|p15 Fig 1|Paleoproterozoic|Paleoproterozoic|Geological province: Gawler Craton.||||||
23856|Myola Volcanics|71799|5|Briefly described|p150 fig 2|Statherian|Statherian|Eastern Gawler Craton.|ca 1875 Ma|||Overlain by the Wallaroo Group.|Silicic volcanics, porphyry.|
23856|Myola Volcanics|71859|5|Briefly described|p3, p6|Paleoproterozoic|Paleoproterozoic|||||||
23856|Myola Volcanics|71862|6|Mentioned|p3|||||||||
23856|Myola Volcanics|72058|6|Mentioned|p171-p172|||Middleback Ranges, Gawler Craton. Associated with a period of intracontinental rifting.|~1790 Ma||||Rhyolitic volcanics.|
23856|Myola Volcanics|72090|6|Mentioned|p8, p10|Statherian|Orosirian|Gawler Craton.|c. 1865-1740 Ma|||||
23856|Myola Volcanics|72459|6|Mentioned|p51|Palaeoproterozoic|Palaeoproterozoic|Lincoln Domain.|1791 +/- 4 Ma|||||
23856|Myola Volcanics|72462|6|Mentioned|p3|Paleoproterozoic|Paleoproterozoic|Gawler Craton.||||||
23856|Myola Volcanics|72463|6|Mentioned|p2|Paleoproterozoic|Paleoproterozoic|||||||
23856|Myola Volcanics|72484|6|Mentioned|p3|||Eyre Peninsula, Gawler Craton.|~1790 Ma.|||||
23856|Myola Volcanics|73026|6|Mentioned|p6-7, p9|Paleoproterozoic|Paleoproterozoic|Eyre Peninsula/Yorke Peninsula.|c. 1790 Ma|||Underlies the Wallaroo Group.|Bi-modal volcanics.|
23856|Myola Volcanics|73027|5|Briefly described|p6-p7, p9|Palaeoproterozoic|Palaeoproterozoic|Eastern Eyre Peninsula/Yorke Peninsula. Associated with the Broadview Schist.|c. 1790 Ma|||||
23856|Myola Volcanics|73030|6|Mentioned|p2148-2149|Statherian|Statherian|Gawler Craton.||||||
23856|Myola Volcanics|73103|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic||||||Interbanded porphyritic rhyolite, rhyodacite, fine-grained felsic and hornblende-rich gneisses and amphibolite.|
23856|Myola Volcanics|73110|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic||||||Interbanded porphyritic rhyolite, rhyodacite, fine-grained felsic and hornblende-rich gneisses and amphibolite.|
23856|Myola Volcanics|73130|6|Mentioned|[poster] Fig.1|Paleoproterozoic|Paleoproterozoic|||||||28-OCT-22
23856|Myola Volcanics|73155|6|Mentioned|p281|Statherian|Statherian|Gawler Craton.|ca. 1790 Ma|||||
23856|Myola Volcanics|73234|6|Mentioned|p19|Statherian|Statherian|Eyre Peninsula, north-eastern.|c. 1790 Ma|||||
23856|Myola Volcanics|73235|6|Mentioned|p53|Statherian|Statherian|Gawler Craton. Spencer region.|1790 Ma|||||
23856|Myola Volcanics|73298|6|Mentioned|p1073|Statherian|Statherian|Gawler Craton.|1790 Ma|||||
23856|Myola Volcanics|73493|6|Mentioned|p716 Fig.3|||Gawler Craton.||||||
23856|Myola Volcanics|73525|5|Briefly described|p19 Fig.13|Statherian|Statherian|Spencer Domain.|1792+/-5 Ma, 1791+/-4 Ma crystallisation age||||Felsic extrusives.|
28840|Myponga Sand|38290|5|Briefly described|p59|||See also Fig.27(a).||||||
28841|Myrtle Springs Formation|22505|5|Briefly described|p7||Adelaidean|||||||
28841|Myrtle Springs Formation|22772|5|Briefly described|Table13.1|Cryogenian|Cryogenian|||||||
28841|Myrtle Springs Formation|22857|5|Briefly described|Tb. 13.1 (insert p70-71)|Torrensian|Torrensian|Of the Burra Group. ||||||
28841|Myrtle Springs Formation|22889|6|Mentioned|p35|Adelaidean|Adelaidean|Parent - Bungarider Subgroup.||||||
28841|Myrtle Springs Formation|23562|5|Briefly described|p295 Fig 2|Cryogenian|Cryogenian|||||||
28841|Myrtle Springs Formation|24175|4|Described|p12|Neoproterozoic|Neoproterozoic|Of the Burra Group. Conformably overlies Skillogalee Dolomite.  Max. thickness: 4000m.||||||13-FEB-08
28841|Myrtle Springs Formation|24176|2|Defined|p38 Appendix|Adelaidean|Adelaidean|See also p11, p25 Tb. 1. Of Burra Group. Grey siltstone and greywacke, minor dolomites and quartzites. Age is Torrensian. Max. thickness: 1070m. Overlies Skillogalee Formation. Geological Province: Mount Painter Province.||||||13-FEB-08
28841|Myrtle Springs Formation|24321|5|Briefly described|Map legend|Adelaidean|Adelaidean|Parent: Burra Group.||||||13-FEB-08
28841|Myrtle Springs Formation|24546|5|Briefly described|p2 - 3 Fig.2|Neoproterozoic|Neoproterozoic|Of Burra Group. Geological Province: Adelaide Fold Belt.||||||16-JAN-08
28841|Myrtle Springs Formation|24593|5|Briefly described|p614|||Of the Burra Group. Geological Province: Mount Painter Inlier.||||||13-FEB-08
28841|Myrtle Springs Formation|30176|6|Mentioned|Map legend|Adelaidean|Adelaidean|Torrensian||||||
28841|Myrtle Springs Formation|30801|6|Mentioned|p5|||Torrensian. Table P5-6||||||
28841|Myrtle Springs Formation|30807|6|Mentioned|p103|||Suggested map symbol||||||
28841|Myrtle Springs Formation|32724|6|Mentioned|Fig.1|||Torrensian. Correlation||||||
28841|Myrtle Springs Formation|33224|6|Mentioned|Fig.38|||Photo||||||
28841|Myrtle Springs Formation|33474|6|Mentioned|Fig.2|||||||||
28841|Myrtle Springs Formation|35255|6|Mentioned|p13|||||||||
28841|Myrtle Springs Formation|36733|6|Mentioned|Table 1|||||||||
28841|Myrtle Springs Formation|37371|6|Mentioned|p382|||See also P377||||||
28841|Myrtle Springs Formation|37461|6|Mentioned|Table 5.I|||||||||
28841|Myrtle Springs Formation|38157|6|Mentioned|Table III|||||||||
28841|Myrtle Springs Formation|38926|5|Briefly described|p39|||||||||
28841|Myrtle Springs Formation|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Torrensian||||||
28841|Myrtle Springs Formation|41400|6|Mentioned|p27|||||||||
28841|Myrtle Springs Formation|41404|4|Described|p116|||||||||
28841|Myrtle Springs Formation|41405|6|Mentioned|p126|||See also P174||||||
28841|Myrtle Springs Formation|41526|6|Mentioned|p58|||||||||
28841|Myrtle Springs Formation|42222|5|Briefly described|p14|||||||||
28841|Myrtle Springs Formation|42236|6|Mentioned|Fig.2 P106|||||||||
28841|Myrtle Springs Formation|42237|5|Briefly described|p87|||See also Fig.2||||||
28841|Myrtle Springs Formation|42238|6|Mentioned|p73|||||||||
28841|Myrtle Springs Formation|43052|5|Briefly described|p183,Table 6.1|||Of Burra Group.||||||13-FEB-08
28841|Myrtle Springs Formation|60718|5|Briefly described|p49 Fig. 2|Adelaidean|Adelaidean|Geological Province: Adelaide Geosyncline. See also p51 Fig. 3, p54.||Of Bungarider Subgroup.||||15-APR-11
28841|Myrtle Springs Formation|60955|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Of the Burra Group. Grey-green siltstones.||||||
28841|Myrtle Springs Formation|65925|5|Briefly described|p124 Fig.3.|||||Unit in Burra Group.|||Green siltstone, sandstone.|
28841|Myrtle Springs Formation|66109|6|Mentioned|p191, 195, 198, 202-203|Proterozoic|Proterozoic|Optical photomicrographs, Raman kerogen images, and confocal laser scanning micrographs of bona fide microfossils and pseudofossils.|~800 Ma.|||||
28841|Myrtle Springs Formation|66884|1|Redefined|p36-44 incl Figs.2-4|||Revised definition subdivided into two unnamed members: lower member and upper member. Age: upper (or Late) Torrensian. Type localities/sections provided for both members. Thickness: lower member is up to 1100 m and upper member is up to 335 m. Old Mount North West Member and lower member of Myrtle Springs Formation encompass strata previously defined as uppermost Burra unit (Coats 1973), Burra Group (Forbes and Coats 1963; Forbes et al. 1965; Forbes 1990) and Myrtle Springs Formation (Preiss 1986; Belperio 1987, 1990; Forbes 1988; Dyson 2000).||Bungarider Subgroup||Disconformably overlies the Old Mount North West Member; conformably overlies Skillogalee Dolomite; upper member is overlain by Wilyerpa Formation.|Upper member: green siltstone; lower member: interbedded subordinate grey quartzite and dolomite typify type locality.|14-DEC-16
28841|Myrtle Springs Formation|69019|4|Described|p41, p46.|Neoproterozoic|Neoproterozoic|Defined by Coats (1973); 2 new Members erected by Hearon et al. (2010) do not occur on the Map. Type section along the Aroona Dam pipeline, 4 km SW of Copley, where it is 1,100 m thick.||Unit in Bungarider Subgroup.||Conformably overlies Skillogalee Dolomite. Is overlain unconformably by Wilyerpa Formation.|Dark grey-green silty slate with minor feldspathic quartzite and greywacke; minor dolomitic quartzite and arkose intervals.|
28841|Myrtle Springs Formation|70384|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Adelaide Geosyncline. Shallow-marine deposits.  Age shown more specifically as Torrensian [Cryogenian].||Bungarider Subgroup.|||Dark grey-green siltstone; minor feldspathic quartzite and greywacke; thin-bedded minor dolomitic quartzite and arkose, cream and dark grey; mudcracks, ripple marks, wavy lamination, stromatolites.|18-JAN-19
28841|Myrtle Springs Formation|72456|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Marree 1:250k map sheet. |||||Siltstone, green; minor quartzite and dolomite.|
82978|Namba Formation, lower member|73251|4|Described|p39, p42, p44-45, p51-52, p57, p59-61|||Of Callen (1977). Cyclic deposition with variations in the relative abundance of smectite to illite. Contains Namba [organic] facies 1.|||||Includes black, indurated, lamosite-type oil shale and whitish palygorskitic dolomite.|
82980|Namba Formation, upper member|73251|4|Described|p39, p41-42, p45, p52, p55, p57, p60-61|||Of Callen (1977). Less smectite than the 'lower member' but has a corresponding increase in white mica. Present only within the Poontana Trough; intersected at Wooltana 1 and Wertaloona 1 drillholes. Maximum thickness: 85.2 m. Contains Namba [organic] facies 2. Basal conglomerate fines up to dolomitic palygorskitic claystone.|||||Dolomitic palygorskitic claystone and conglomerate.|
80054|Nancatee Granite|70405|4|Described|p36|Paleoproterozoic|Paleoproterozoic|Olary Domain, Curnamona Province. Age poorly constrained.|1710 Ma - 1720 Ma|Kalabity Supersuite||Intrudes Peryhumuck Formation|Lenticular body of fine grained muscovite bearing (presumed) S type granite. Some foliation is present and is concordant with bedding parallel foliation of host metasediments.|21-SEP-17
41179|Nangeela Formation|50154|2|Defined|p22, p52, p62|Early Cambrian|Early Cambrian|Of the Moralana Supergroup. Interlayered with the Truro Volcanics. Includes Steep Bank Greywacke Member and Warrock LImestone Member. Correlates with the Normanville and Kanmantoo groups. Geological Province: Glenelg Zone, Delamerian Fold Belt.||||||15-SEP-04
41179|Nangeela Formation|50156|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of Moralana Supergroup. Overlain by Eumeralla Formation. Black graphite slate with pyrite; black dolomitic slate with pyrite; chlorite-sericite slate and metasiltstone; thin greywacke interbeds.||||||25-JUN-04
41179|Nangeela Formation|50157|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of Moralana Supergroup. Black graphite slate with pyrite; black dolomitic slate with pyrite; chlorite-sericite slate and metasiltstone; thin greywacke interbeds.||||||24-JUN-04
41179|Nangeela Formation|50158|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of Moralana Supergroup. Includes: Warrock Limestone Member, Steep Bank Greywacke Member. Black graphitic and dolomitic slate with pyrite; chlorite-sericite slate and metasiltstone; thin greywacke interbeds.||||||
41179|Nangeela Formation|50159|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of Moralana Supergroup. Black graphite slate with pyrite; black dolomitic slate with pyrite; chlorite-sericite slate and metasiltstone; thin greywacke interbeds.||||||
41179|Nangeela Formation|50160|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of Moralana Supergroup. Includes: Warrock Limestone Member, Steep Bank Greywacke Member. Black graphitic and dolomitic slate with pyrite; chlorite-sericite slate and metasiltstone; thin greywacke interbeds.||||||16-JUN-04
41179|Nangeela Formation|50161|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of Moralana Supergroup. Includes Steep Bank Greywacke Member and Warrock Limestone Member. Black graphite slate with pyrite; black dolomitic slate with pyrite; chlorite-sericite slate and metasiltstone; thin greywacke interbeds.||||||22-JUN-04
41179|Nangeela Formation|50162|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of Moralana Supergroup. Black graphite slate with pyrite; black dolomitic slate with pyrite; chlorite-sericite slate and metasiltstone; thin greywacke interbeds.||||||
41179|Nangeela Formation|50163|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of Moralana Supergroup. Overlain by Duddo Limestone. Black graphite slate with pyrite; black dolomitic slate with pyrite; chlorite-sericite slate and metasiltstone; thin greywacke interbeds.||||||25-JUN-04
41179|Nangeela Formation|50164|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Overlain by Otway Group. Of Glenelg River Metamorphic Complex (Moralana Supergroup).||||||25-JUN-04
41179|Nangeela Formation|66002|5|Briefly described|p4 Tb.1|Cambrian|Cambrian|Of Moralana Supergroup. Includes Steep Bank Greywacke Member and Warrock Limestone Member. Defined  by Morand et al. 2003||||||
41179|Nangeela Formation|68116|5|Briefly described|Appendix, Map 29.|Middle Cambrian|Early Cambrian||||||Black graphitic slate with pyrite; black dolomitic slate with pyrite; grey to green chlorite-sericite slate and metasiltstone; thin greywacke interbeds.|
41179|Nangeela Formation|71593|4|Described|p8, p12, p20-p22, p102, p133, p150|Cambrian|Cambrian|Glenelg Zone.|||Includes the Steep Bank Greywacke Member.|Equivalent (in part) to the Kanmantoo Group.|Shale marl and carbonate rich units including slates.|
41179|Nangeela Formation|73093|5|Briefly described|map legend|Cambrian|Cambrian||||||Black graphitic and dolomitic slate with pyrite; grey to green chlorite-sericite slate and metasiltstone; thin greywacke interbeds.|09-DEC-21
24419|Napoleon Megabreccia Member|22889|6|Mentioned|Table 1 on p32|Adelaidean|Adelaidean|Parent - Skillogalee Dolomite of the Mundallio Subgroup.||||||
24419|Napoleon Megabreccia Member|39348|6|Mentioned|Map legend|Adelaidean|Adelaidean|Torrensian||||||
24419|Napoleon Megabreccia Member|40225|6|Mentioned|Map sheet|||||||||
24419|Napoleon Megabreccia Member|40294|3|Fully described|p38|||||||||
24419|Napoleon Megabreccia Member|41404|4|Described|p105|||||||||
24419|Napoleon Megabreccia Member|42222|6|Mentioned|Table 1 P5|||||||||
24419|Napoleon Megabreccia Member|43052|5|Briefly described|p179,Table 6.1|||of Skillogalee Dolomite||||||
24419|Napoleon Megabreccia Member|60959|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Of the Skillogalee Dolomite. Unsorted clasts of blue-grey dolomite and siltstone in dolomitic and silty matrix.||||||
22509|Narana Formation|22746|4|Described|Fig.3 p515, p525|Neoproterozoic III|Neoproterozoic III|||||||
22509|Narana Formation|22802|6|Mentioned|p872|||Officer Basin||||||
22509|Narana Formation|22922|6|Mentioned|34|||||||||
22509|Narana Formation|23282|2|Defined|p65||Neoproterozoic|Of Zang (1995). May correlate with Pound Subgroup in the Adelaide Fold Belt, the equivalent in Amadeus Basin is the lower Arumbera Sandstone. Age: Precambrian/Neoproterozoic, late Marinoan Epoch. of Ungoolya Group. In Officer Basin.||||||15-FEB-07
22509|Narana Formation|23479|5|Briefly described|p26|||Of Ungoolya Group. Geological Province: Gawler Craton.||||||
22509|Narana Formation|23524|5|Briefly described|p221 Fig. 3|Neoproterozoic|Neoproterozoic|||||||
22509|Narana Formation|23981|5|Briefly described|p10 Fig. 5|Precambrian|Precambrian|Geological Province: eastern Officer Basin.||||||
22509|Narana Formation|24112|5|Briefly described|p254 Fig.2|Neoproterozoic|Neoproterozoic|Of the Ungoolya Group. Geological Province: Officer Basin||||||
22509|Narana Formation|43743|6|Mentioned|Fig.2,p33||Neoproterozoic|||||||
22509|Narana Formation|61732|3|Fully described|p5 Tb. 1, p65-67|Ediacaran|Ediacaran|Of Ungoolya Gp. Includes Munta Lst. and Mena Mudst.Members. Overlies Munyarai Fm or Tanana Fm; unconform overlies lower Dey Dey Mudst. Unconform overlain by Marla Gp. Thick: <1500m. Geol.Prov: Officer Basin. See p58 Fig. 22, p134.||||||07-FEB-11
22509|Narana Formation|63397|2|Defined|32|Neoproterozoic III|Neoproterozoic III|Of the Ungoolya Group. Type section in text. Dark-grey silty mudstone, silty limestone with minor sandstone and mass flow breccia. Max thickness: 1500m+. Unconformably overlies: Munyarai Formation and Tanana Formation.||||||
22509|Narana Formation|64794|4|Described|p238 fig 2, p240 Tb.1, p242 fig 3 |Ediacaran|Ediacaran|See also p245, p275. Canyon-fill deposits on underlying Tanana Formation. Barren of palynomorphs.||Ungoolya Group||Overlies Tanana Formation unconformably.|Three parts: upper 43m grey fine-grained limestone; middle 44m thin limestone beds in dark-grey calcareous mudstone; lower 155m thick dark grey-green silty shale with minor thin beds of paler calcareous siltstone or very fine grained sandstone.|
22509|Narana Formation|64797|6|Mentioned|p153 Fig.2|Ediacaran|Ediacaran|Officer Basin. Lithology/rank not shown on diagram.||||||
22509|Narana Formation|65416|6|Mentioned|p146.|||Suggested by Perincek (1996) to post-date the Petermann Ranges Orogeny.||||||
22509|Narana Formation|66569|5|Briefly described|p861 fig.2,|Ediacaran|Ediacaran|Oof Ungoolya Group; unconformably overlies Munyarai Formation.||||||
22509|Narana Formation|68269|6|Mentioned|p674|Ediacaran|Ediacaran|Officer Basin.||Ungoolya Group||Unconformably underlain by Munyarai Formation.|Mudstone dominated.|
22509|Narana Formation|72478|6|Mentioned|p8|Marinoan|Marinoan|Officer Basin.|c. 575 Ma|Ungoolya Group|Includes the Munta Limestone Member and the Mena Mudstone Member.|Unconformably overlies Tanana Formation.||24-MAR-21
22509|Narana Formation|73099|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Officer Basin.||Ungoolya Group.|Munta, Mena, Mudstone Members.|Overlies Tanana Formation. Is overlain by Relief Sandstone or Observatory Hill Formation (Marla Group).|Grey, interbedded siltstone, claystone, limestone and minor very fine-grained sandstone and intraformational conglomerate; slump structures and calcite veins.|
33819|Narcoonowie Formation|62537|6|Mentioned|p191 Fig.2. |Ordovician|Late Cambrian|Warburton Basin.||||||
33819|Narcoonowie Formation|63056|5|Briefly described|p80, p81 Fig. 2|||Lowstand fan, laterally equivalent to Innamincka Formation. Geological Province: Warburton Basin.||||||06-FEB-07
33819|Narcoonowie Formation|65489|5|Briefly described|p39, p96, p119-120|Early Ordovician|Late Cambrian|Eastern Warburton Basin. Potential reservoir sandstones.||||Overlies Lycosa Formation. Lateral equivalent of Innamincka Formation.|Turbidites.|
33819|Narcoonowie Formation|68731|6|Mentioned|p170 Fig 3.83|Early Ordovician|Late Cambrian|Lowstand fan. Upper Member: shelf carbonates and siliciclastics, trilobites and conodonts.||||||
33819|Narcoonowie Formation|69982|2|Defined|p17-19, p23-24, p28-29, p45, p56, p60-61|Ordovician|Late Cambrian|See also p157, p165, Appendix 1. New name. Type section is the interval from 1861.72 to 1996.40 m in Narcoonowie 1 well. Warburton Basin. 135 m thick in type sect. Deposition by debris flow and grain flow after slope front erosion. Brief thin section descriptions. Composite logs shown.||Unit in Dullingari Group.||Overlies Lycosa Formation.|Thinly interbedded sandstone, greywacke, siltstone and shale, and minor pebbly sandstone or sandy breccia.|12-NOV-15
33819|Narcoonowie Formation|73244|6|Mentioned|p86|Ordovician|Ordovician|Warburton Basin. Lowstand fan environment.||||||
33819|Narcoonowie Formation|73479|5|Briefly described|p156 Fig.2, p157|Ordovician|Cambrian|Warburton Basin. Lowstand fan depositional environment.|ca 490 Ma|||Underlies Innamincka Fornation||
37331|Nargoon Group|23309|4|Described|p40, p5 Fig. 1.3|Cambrian|Cambrian|||||||22-FEB-10
37331|Nargoon Group|24311|5|Briefly described|p1059 Fig. 2|Cambrian|Cambrian|||||||
37331|Nargoon Group|24551|4|Described|p80|Late Cambrian|Late Cambrian|Intruded by Bushy Creek Granite.||||||03-AUG-05
37331|Nargoon Group|50154|2|Defined|p24, p47, p72, p143|Late Cambrian|Middle Cambrian|Overlies the Mount Stavely Volcanics. Unconformably overlain by the Grampians Group and quartz-cobble conglomerate of the Renmark Group. Geological Province: Grampians-Stavely Zone, Delamerian Fold Belt.||||||15-SEP-04
37331|Nargoon Group|50155|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Marine turbidites||||||22-MAY-13
37331|Nargoon Group|50156|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Marine turbidites: cleaved quartz wacke and slate; thin bedded.||||||22-MAY-13
37331|Nargoon Group|50157|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Marine turbidites: cleaved quartz wacke and slate; thin bedded.||||||22-MAY-13
37331|Nargoon Group|50158|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Unconformably overlain by Grampians Group. Marine turbidites: cleaved quartz wacke and slate; thin bedded.||||||22-MAY-13
37331|Nargoon Group|50159|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Overlain by Grampians Group and Shepparton Formation. Marine turbidites: cleaved quartz wacke and slate; thin bedded.||||||22-MAY-13
37331|Nargoon Group|50160|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Marine turbidites: quartz wacke and slate.||||||22-MAY-13
37331|Nargoon Group|50161|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Marine turbidites: cleaved quartz wacke and slate; thin bedded.||||||22-MAY-13
37331|Nargoon Group|50162|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Marine turbidites: cleaved quartz wacke and slate; thin bedded.||||||22-MAY-13
37331|Nargoon Group|50163|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Marine turbidites: cleaved quartz wacke and slate; thin bedded.||||||22-MAY-13
37331|Nargoon Group|60451|6|Mentioned|p21, Fig. 7|||||||||
37331|Nargoon Group|60454|5|Briefly described|Map Legend|Cambrian|Cambrian|Geological Province: Delamerian Fold Belt. Includes: Glenthompson Sandstone.||||||22-MAY-13
37331|Nargoon Group|60456|5|Briefly described|Map Legend|Cambrian|Cambrian|Geological Province: Delamerian Fold Belt. Includes: Glenthompson Sandstone.||||||22-MAY-13
37331|Nargoon Group|60457|5|Briefly described|Map Legend|Cambrian|Cambrian|Includes: Glenthompson Sandstone. Geological Province: Delamerian Fold Belt.||||||22-MAY-13
37331|Nargoon Group|60458|5|Briefly described|Map Legend|Cambrian|Cambrian|Geological Province: Delamerian Fold Belt. Includes: Glenthompson Sandstone.||||||22-MAY-13
37331|Nargoon Group|60459|5|Briefly described|Map Legend|Cambrian|Cambrian|Geological Province: Delamerian Fold Belt. Includes: Glenthompson Sandstone.||||||22-MAY-13
37331|Nargoon Group|62755|5|Briefly described|p876 Fig. 1|Cambrian|Cambrian|Includes the Glenthompson Sandstone.||||||
37331|Nargoon Group|64314|5|Briefly described|p495 Fig. 2a|Cambrian|Cambrian|||||||
37331|Nargoon Group|66002|5|Briefly described|p4 Tb.1|Cambrian|Cambrian|Includes Glenthompson Sandstone. Defined by VandenBerg et al. 2000 p38.||||||
37331|Nargoon Group|67104|6|Mentioned|p635|||May correlate with the Mariner Group in Antarctica.||||||
37331|Nargoon Group|68116|5|Briefly described|Appendix, Maps 29, 30.|Late Cambrian|Early Cambrian||||||Quartz wacke and slate; thin-bedded.|
37331|Nargoon Group|68194|6|Mentioned|p21||||||Includes Glenthompson Sandstone.|||
37331|Nargoon Group|70211|5|Briefly described|p3, p35|||VandenBerg et al. (2000).|||Glenthompson Sandstone.|Overlies Mount Stavely Volcanic Complex. Is overlain unconformably by Grampians Group.||
37331|Nargoon Group|70493|6|Mentioned|p56|Late Cambrian|Late Cambrian|Grampians-Stavely Zone, Lachlan Orogen.||||Overlies Mount Stavely Volcanic Complex. Is overlain unconformably by Grampians Group.||
37331|Nargoon Group|70877|4|Described|p10, p13-p21, p167, p196||Ediacaran|Grampians-Stavely Zone. Horsham 1:250k and NHill 1:100k Map sheets. Previously interpreted to include the Glenthompson Sandstone, in this volume the old Glenthompson Sandstone is separated from the younger Nargoon Group. SHRIMP age derived from this volume and represents a maximum possible age of deposition. Petrography, zircon morphology and SHRIMP U-Pb results of an undifferentiated sample of this group is discussed in detail.|552 +/- 8 Ma (SHRIMP U-Pb)|||Overlain by the Grampians Group.|Sandstone and siltstone; dominated by albitised feldspar and chlorite, contains detrital amphibole and garnet.|
37331|Nargoon Group|70967|6|Mentioned|p9, 11, 18-19|||Grampians-Stavely Zone. Sedimentary rocks. Deformed during the Delamerian Orogeny.|||Glenthompson Sandstone.|||
37331|Nargoon Group|71593|4|Described|p1, p8, p12, p19, p22|Cambrian|Cambrian|Delamerian Orogen, Grampians-Stavely Zone. A type locality is mentioned but not provided. Petrography briefly discussed. See also p24, p26, p43, p72, p102, p133, p188-p189, p194.||||Faulted against the Glenelg River Metamorphic Complex. Unconformably overlain by the Grampians Group.|Graphitic slate, chert and cleaved sandstone with sedimentary features such as low angle cross-bedding.|
37331|Nargoon Group|72445|5|Briefly described|p8, p10, p17, p18; App.1, App.2, App.5|Early Cambrian|Early Cambrian|Shown as part of the target basement. App.2 is a .csv format file. Identified in Stavely 05,14. Overlies the Stavely arc. See also app 7 p6.|||Includes Glenthompson Sandstone.|Shown as underlying Renmark Group with sharp contact. Overlain by the Grampians Group.|Fine-grained sandstone with 0.2-6.3 m siltstone intervals. Variably weathered, fine to medium grained sandstone with 0.1-1.5 m siltstone intervals towards base.|15-OCT-20
37331|Nargoon Group|73059|6|Mentioned|p1059|Late Cambrian|Late Cambrian|Grampians-Stavely Zone.||||||
37331|Nargoon Group|73093|5|Briefly described|map legend|Cambrian|Cambrian||||||Marine turbiditic, cleaved quartz wacke and slate.|09-DEC-21
37331|Nargoon Group|73430|6|Mentioned|p493||||||||Variably deformed siliciclastic sediment sequences.|
23865|Narlaby Formation|24606|5|Briefly described|p956, p959|Early Pliocene|Early Pliocene|Overlies the Garford Formation. Geological Province: Eucla Basin||||||
23865|Narlaby Formation|42816|5|Briefly described|p26|||||||||
23865|Narlaby Formation|44133|5|Briefly described|p185, 180 Fig. 10.22|Pliocene|Pliocene|Geological Province: Eucla Basin. Overlies: Garford Formation. Thickness: 60m. Fluvial to ?estuarine fine to medium grained, moderately well sorted sand with little clay. Partly silicified, iron-stained and varicoloured.||||||18-JAN-22
23865|Narlaby Formation|61234|6|Mentioned|p6, p7 Fig 4.|Pliocene|Miocene|Age: Late Miocene and Early Pliocene.||||||
23865|Narlaby Formation|64646|6|Mentioned|p23 Fig. 3, p24 Fig. 4|Pliocene|Pliocene|Geological Province: Gawler Craton.||||||08-FEB-10
23865|Narlaby Formation|65194|5|Briefly described|p171|||Narlaby Palaeovalley. Fluvial fine- to medium-grained, moderately to well sorted sands; partly silicified and iron-stained. Overlies Garford Formation. Associated with uranium mineralisation.||||||
23865|Narlaby Formation|67462|5|Briefly described|Map legend.|Pliocene|Pliocene|Eucla Basin.||||||
23865|Narlaby Formation|68715|6|Mentioned|p30 Fig.5|Pliocene|Pliocene|Bunda Plateau and SW Gawler Craton, Eucla Basin.||||||
23865|Narlaby Formation|69004|6|Mentioned|p28|||||||Overlies the Pidinga Formation.||
23865|Narlaby Formation|69598|6|Mentioned|p9|Early Pliocene|Early Pliocene|||||Overlies the Garford Formation. Overlain by the Ilkina Formation.||
23865|Narlaby Formation|69649|5|Briefly described|p32|||Up to 60m thick.|||||Fluvial to estuarine, fine- to medium-grained, moderately to well sorted sand with minor clay.|
27518|Naryilco Silcrete|30804|6|Mentioned|Table 1|||||||||
27518|Naryilco Silcrete|30919|6|Mentioned|Map legend|Oligocene|Oligocene|Prob. Oligocene||||||
27518|Naryilco Silcrete|31532|4|Described|Table 1|||||||||
27518|Naryilco Silcrete|61155|5|Briefly described|p17||Early Oligocene|Geological region: Oodnadatta area.||||||
78881|Neales Formation|67578|5|Briefly described|p343, 347|Quaternary|Quaternary|Age determined using thermoluminescence. Ranges in thickness between 1.5-6m. Two main fluvial facies are recognised: main-channel (informally called Warmakidyaboo Beds) and ephemeral channel facies. These interdigitate with lacustrine (Ghost Yard Beds)/deltaic, unconfined channel (Piarooka Beds) and aeolian facies.|Minimum age of 150 ka.|||Unconformably overlies Eyre and Etadunna Formations.|Basal gravels (reworked Etadunna Formation), trough-bedded sand and fine gravel, horizontally-bedded sand, silt and clay sequences.|
31401|Nepouie Subgroup|22510|2|Defined|table1p37,40,41|||Type section: As for the constituent formations listed below. A useful reference section is along Nepouie Creek, between 139degrees21'58"E, 30degrees28'56"S and 139degrees21'17"E, 30degrees28'14"S, where the thickness is ~400 m. where the thickness is ~400 m.. Age: 750+/-63 Ma (Webb and Coats, 1980).  Disconformably overlies Yudnamutana Subgroup; disconformably overlain by Upalinna Subgroup.|||Serle Conglomerate, Tapley Hill Formation and its consitituent members.|||26-NOV-22
31401|Nepouie Subgroup|23477|5|Briefly described|p49 Fig 3|Neoproterozoic|Neoproterozoic|Geological Province: Curnamona Province.||||||
31401|Nepouie Subgroup|60718|5|Briefly described|p49 Fig. 2|Adelaidean|Adelaidean|Geological Province: Adelaide Geosyncline.||Of Umberatana Group.||Includes Tapley Hill Formation and Serle Conglomerate.||15-APR-11
31401|Nepouie Subgroup|60953|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Of the Umberatana Group.||||||
31401|Nepouie Subgroup|60959|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Of the Umberatana Group.||||||
31401|Nepouie Subgroup|61108|5|Briefly described|map legend|Adelaidean|Adelaidean|Of the Umberatana Group. Mainly interglacial. Marine and marginal marine siltstone and sandstone; oolitic, sandy and stromatolitic limestone.||||||06-JUN-05
31401|Nepouie Subgroup|61238|5|Briefly described|p44 Fig. 1|Neoproterozoic|Neoproterozoic|Of the Umberatana Group.||||||14-MAY-07
31401|Nepouie Subgroup|61732|5|Briefly described|p28 Fig. 13|Sturtian|Sturtian|Of the Umberatana Group. Includes the Tapley Hill Formation and Brighton Limestone. Geological Province: Adelaide Rift Complex.||||||07-FEB-11
31401|Nepouie Subgroup|62085|6|Mentioned|p19 Fig.4|Cryogenian|Cryogenian|||Unit in Umberatana Group.|||Siltstone, dolomite.|
31401|Nepouie Subgroup|62592|5|Briefly described|p20 Fig.2.4, p50 Table 5.1, pp57-58.|Sturtian|Sturtian|A post-glacial transgressive-regressive sequence, representing the first sag-phase deposition in the Adelaide Geosyncline. Colour scheme shown for interpretation of Curnamona seismic sections. Written as SubGroup.||Unit in Umberatana Group.|Includes Tapley Hill Formation and Wockerawirra Dolomite.|Disconformably overlies Yudnamutana Subgroup. Is disconformably overlain by Upalinna Subgroup.||
31401|Nepouie Subgroup|62724|5|Briefly described|p16 Fig. 2|Neoproterozoic|Neoproterozoic|Siltstone. Geological Province: Curnamona Province.||||||07-FEB-11
31401|Nepouie Subgroup|63102|5|Briefly described|p8|Neoproterozoic|Neoproterozoic|Geological province: Curnamona Province.|||||Siltstone.|
31401|Nepouie Subgroup|64846|5|Briefly described|p198|Cryogenian|Cryogenian|Interglacial succession.||Of the Umberatana Group. |Includes Tapley Hill Formation and Balcanoona Formation.|||
31401|Nepouie Subgroup|65493|5|Briefly described|p910, p909 Fig 2|Cryogenian|Cryogenian|Of the Umberatana Group. Unconformably overlies the Yudnamutana Subgroup. Includes Tapley Hill Formation, Balcanoona Formation. Interglacial deposit.||||||
31401|Nepouie Subgroup|67180|4|Described|p600, p601 Fig.1, p602 Fig.2|Cryogenian|Cryogenian|Sturtian age. Defined by Preiss et al. (1998).||Unit in Umberatana Group|Includes Angepena Formation, Balcanoona Formation, Tapley Hill Formation|Underlies the Upalinna Subgroup, overlies the Yudnamutana Subgroup.||
31401|Nepouie Subgroup|67870|5|Briefly described|p9|Neoproterozoic|Neoproterozoic|Adelaide Rift System.||Umberatana Group.|Tapley Hill, Balcanoona Formations.|||
31401|Nepouie Subgroup|67979|4|Described|p528, p531 Fig.2, p542, 543-545|Sturtian||Interglacial succession (Preiss et al. 1998). Nepouie-Upalinna Subgroup boundary now proposed to coincide with the Sturtian-Marinoan Series boundary in Northern & Central Flinders Ranges, on basis of new correlations.||Umberatana Group|Includes Tapley Hill Formation, Balcanoona Formation and Angepena Formation|Is overlain by Upalinna Subgroup; overlies Yudnamutana Subgroup||22-SEP-14
31401|Nepouie Subgroup|68068|5|Briefly described|Map legend|Marinoan|Marinoan|Adelaide Geosyncline.||Unit in Umberatana Group.|Includes Balcanoona Formation.|||
31401|Nepouie Subgroup|69019|5|Briefly described|p41, p46-49.|Neoproterozoic|Neoproterozoic|Preiss et al. (1998); partially replaces Farina Subgroup (name abandoned). Late Sturtian portion of northern Adelaide Geosyncline sedimentation. Occurs in Flinders and Willouran Ranges. ||Unit in Umberatana Group.|Includes Serle Conglomerate, Tapley Hill Formation, Balcanoona Formation.||Overall transgressive-regressive succession of conglomerate, sandstone, siltstone, shale and dolomite.|
31401|Nepouie Subgroup|69023|5|Briefly described|p64-72|Neoproterozoic|Neoproterozoic|Defined by Preiss et al. (1998). A Late Sturtian transgression-regression sequence.||Unit in Umberatana Group.|Includes Balcanoona Formation.||Siltstone, shale, dolomite, sandstone and conglomerate.|
31401|Nepouie Subgroup|70031|4|Described|p245|Cryogenian|Cryogenian|Adelaide Geosyncline. Lower interglacial succession; waning stages of Sturtian glaciation.||Unit of Umberatana Group.|Includes Brighton Limestone and Tapley Hill Formation.|Overlain conformably by Upalinna Subgroup/Angepena Formation. Underlain by .||
31401|Nepouie Subgroup|70323|5|Briefly described|p213|Cryogenian|Cryogenian|Central Flinders Ranges, Adelaide Geosyncline. |c. 650 Ma|Unit of Umberatana Group.|Includes Tapley Hill Formation.|Underlain by Yudnamutana Group/Wilyerpa Formation.||
31401|Nepouie Subgroup|70334|5|Briefly described|p20,47|||Geological province: Gawler Craton. Of Adelaide Geosyncline and Stuart Shelf. ||Unit of Umberatana Group.|Includes Brighton Limestone and Tapley Hill Formation.|Overlain unconformably by Whyalla Sandstone or Tapley Hill Formation.||
31401|Nepouie Subgroup|70384|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Adelaide Geosyncline.  Age shown more specifically as Sturtian [Cryogenian].||Of Umberatana Group.|Includes Serle Conglomerate; Tapley Hill, Balcanoona Formations.|Unconformably overlies Yudnamutana Subgroup. Is overlain unconformably by Upalinna Subgroup.||23-JAN-19
31401|Nepouie Subgroup|70405|6|Mentioned|p14 figure 6|Neoproterozoic|Neoproterozoic||||||Siltstone.|
31401|Nepouie Subgroup|70657|6|Mentioned|p9 Fig.3|Neoproterozoic|Neoproterozoic||||||Siltstone.|
31401|Nepouie Subgroup|70658|6|Mentioned|p14|Neoproterozoic|Neoproterozoic||||||Siltstone.|
31401|Nepouie Subgroup|70819|6|Mentioned|p11, 13, 29|Neoproterozoic|Neoproterozoic|Clare Valley.||Umberatana Group.|Tapley Hill Formation.|Overlies Yudnamutana Subgroup.||
31401|Nepouie Subgroup|71129|6|Mentioned|p107|Cryogenian|Cryogenian|Of Stuart Shelf. Deposited during ensuing glacio-eustatic sea-level rise after Sturt Glaciation.||Of the Umberatana Group.|Includes Tapley Hill Formation.|Overlain by the Upalinna Subgroup.||13-NOV-19
31401|Nepouie Subgroup|71895|6|Mentioned|APP4. p4, |||Punt Hill Region.||||||
31401|Nepouie Subgroup|73188|6|Mentioned|p316|Neoproterozoic|Neoproterozoic|Mount Lofty Ranges.||Umberatana Group|Brighton Limestone, Tapley Hill Formation|||
31401|Nepouie Subgroup|73236|6|Mentioned|p36, p38|Cryogenian|Cryogenian|Marine sedimentary rocks.||Umberatana Group, Heysen Supergroup|Brighton Limestone, Tapley Hill Formation|Underlain by Sturt Tillite (Yudnamutana Subgroup). Overlain by Angepena Formation (Upalinna Subgroup).||
31401|Nepouie Subgroup|74367|5|Briefly described|p3, p7 Fig.6, p8, p19|Cryogenian|Cryogenian|||Umberatana Group|Tapley Hill Formation|||
25336|Neptune Formation|22485|4|Described|p51 , Fig 2 & p53|Early Cretaceous|Early Cretaceous|||||||
25336|Neptune Formation|22663|5|Briefly described|S97-1 and 2 p3||Early Cretaceous|||||||01-MAR-10
25336|Neptune Formation|23792|5|Briefly described|Fig.D4|Berriasian|Berriasian|Equivalent to Southern Right supersequence. Overlies Echidna Formation. Overlain by Lower Borda Formation. Geological Province: Bight Basin.||||||
25336|Neptune Formation|24201|5|Briefly described|p373 Fig. 2|Berriasian|Berriasian|||||||
25336|Neptune Formation|24338|5|Briefly described|p938 Fig. 2|Berriasian|Berriasian|Overlain by the Borda Formation. Overlies the Echidna Formation. Formation is Fm in text. Geological Province: Bight Basin.||||||
25336|Neptune Formation|24350|5|Briefly described|Fig. 4 Appdx|Berriasian|Berriasian|Part of the Southern Right Supersequence. ||||||
25336|Neptune Formation|24443|5|Briefly described|Fig.7|Berriasian|Berriasian|Overlies Echidna Formation. Overlain by Lower Borda Formation. Geological Province: Bight Basin.||||||
25336|Neptune Formation|24553|5|Briefly described|p37, Figs. 7, and 8|||Geological Province: Duntroon Sub-basin. Marine sands. Contains thick shales which act as a seal. Part of the Southern Right Supersequence.||||||07-FEB-11
25336|Neptune Formation|42545|2|Defined|p5|Barremian||NOT variation on Neptune Group, Antarctica.||||||
25336|Neptune Formation|43026|5|Briefly described|Table 1,p586|||||||||
25336|Neptune Formation|43672|5|Briefly described|p330|Barremian|Valanginian|||||||
25336|Neptune Formation|43814|6|Mentioned|Fig.3, p115|||||||||26-JUN-14
25336|Neptune Formation|44133|5|Briefly described|p140|Barremian|Neocomian|Underlies: Borda Formation. ||||||
25336|Neptune Formation|61544|6|Mentioned|p367 Fig.3. |Berriasian|Berriasian|||||Overlies Echidna Formation. Is overlain by Borda Formation.||26-JUN-14
25336|Neptune Formation|61630|6|Mentioned|p555 Fig. 3, p557|Early Cretaceous|Early Cretaceous|Geological Province: Bright and Duntroon Basins.||||||07-APR-09
25336|Neptune Formation|69297|5|Briefly described|p14 fig 2.4|Valanginian|Berriasian|Duntroon Sub-basin. Deposited in fluvial channel, floodplain and lacustrine environments. Contains good potential seal facies. See also p25 fig 2.9, p58, p60, p63, p64.||||Overlies the Echidna Formation. Overlain by the Borda Formation, Lower.|Shale.|
25336|Neptune Formation|70067|5|Briefly described|Ceduna: Fig.2. Regional: Fig.2|Valanginian|Berriasian|Duntroon Sub-basin, Bight Basin.||||Overlies Echidna Formation. Is overlain by Lower Borda Formation.||
29935|Neuroodla Formation|43052|5|Briefly described|Table 2.1 p27|||Torrens Basin||||||
29935|Neuroodla Formation|44133|5|Briefly described|p187|Late Miocene|Early Miocene|Geological Province: Torrens Basin. Overlies the Cotabena Formation. Correlated with the Etadunna Formation. Thickness: ~250m. ||||||
29935|Neuroodla Formation|60959|5|Briefly described|Map Legend|Miocene|Oligocene|Green-grey to black, argillaceous and white calcareous mudstone; basal carbonaceous clay.||||||
29935|Neuroodla Formation|67870|6|Mentioned|p21, p23|Miocene|Oligocene|||||||
29935|Neuroodla Formation|73234|5|Briefly described|p23|||Torrens Basin. Deposited in terrestrial playa lake and floodplain environments. Contemporaneous with Melton Limestone.||||Possibly equivalent to Sugarloaf Dam Sandstone. Equivalent to Etadunna Formation.|Black argillaceous and white calcareous-dolomitic mudstones and includes very soft, red-brown fine- to medium-grained clayey sandstone.|
23869|Neva Clay Member|22525|5|Briefly described|p37,40||Pleistocene|part of the Ngaltinga Formation.|||||Dominated by grey to olive-green massive clay.|24-AUG-18
23869|Neva Clay Member|41551|6|Mentioned|p465|||||||||
39169|New Cornwall Member|24475|2|Defined|p51|Paleoproterozoic|Paleoproterozoic|Referred to as unnamed unit (Lx1) of Wallaroo Group by Conor (1995). Of Wandearah Formation. Overlain by Wokurna Member.||||||07-NOV-08
39169|New Cornwall Member|60958|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Wandearah Formation.  Carbonate-dominated unit. Layered limestone, dolomite, siltstone, calcareous argillite, calcsilicate, graphitic schist, locally sandstone, conglomerate and albitite. Geological Province: Gawler Craton.||||||07-NOV-08
39169|New Cornwall Member|61121|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Wandearah Formation. Carbonate-dominated unit. Layered limestone, dolomite, siltstone, carlcareous argillite, calcsilicate, graphitic schist, locally sandstone, conglomerate and albitite. Geological Province: Gawler Craton.||||||07-NOV-08
39169|New Cornwall Member|65375|4|Described|p19, pp21-22, p53.|Paleoproterozoic|Paleoproterozoic|Name replaced New Cornwall Formation. Equivalent to the East Kadina Group of Lynch (1982). Interdigitated with minor felsic, intermediate and mafic rocks. Considered to be transitional between Doora and Aagot Members. Contains several wide but low-grade mineralised zones, mainly copper.||Unit in Wandearah Formation.|||Metamorphosed layered limestone, dolomite, laminated calcareous and graphitic argillite and locally sandy argillite.|
39169|New Cornwall Member|65376|6|Mentioned|p101 Fig.3.1.|||||Unit in Wandearah Formation.||||
39169|New Cornwall Member|69748|6|Mentioned|p179-181, 183|Paleoproterozoic|Paleoproterozoic|Moonta-Wallaroo region, Olympic IOGC Province.||Wandearah Formation.|||Limestones.|
38291|Newer Volcanic Group|24383|4|Described|p13, 18|Pleistocene|Late Miocene|Age: 8.5 - 0.1Ma. Underlying Unit: Calivil Formation and Castlemaine Group (unconformable). Max Thickness: <100m. Geological Province: Lachlan Fold Belt.||||||03-FEB-09
38291|Newer Volcanic Group|24384|5|Briefly described|Map legend|Miocene|Eocene|||||||
38291|Newer Volcanic Group|24385|5|Briefly described|Map legend|Miocene|Eocene|||||||
38291|Newer Volcanic Group|24386|5|Briefly described|Map legend|Miocene|Eocene|||||||
38291|Newer Volcanic Group|24387|5|Briefly described|Map legend|Miocene|Eocene|||||||
38291|Newer Volcanic Group|24388|5|Briefly described|Map legend|Pliocene|Eocene|||||||
38291|Newer Volcanic Group|24438|5|Briefly described|p17, p34|Quaternary|Miocene|Lava flows and scoria cones. Covers deep lead drainage system of White Hills Gravel. See Newer Volcanics.|||||Flood basalts, scoria cones.|10-MAY-17
38291|Newer Volcanic Group|24439|5|Briefly described|p7 Fig. 2, p8|Quaternary|Cenozoic|||||||19-NOV-08
38291|Newer Volcanic Group|24440|5|Briefly described|Map legend|||||||||
38291|Newer Volcanic Group|50155|5|Briefly described|Map Legend|Pleistocene|Miocene|Basaltic lava flow, scoria, ash.||||||
38291|Newer Volcanic Group|50156|5|Briefly described|Map Legend|Pleistocene|Miocene|Lava flows: olivine basalt, tholeiitic; moderately to well vesiculated.||||||03-FEB-09
38291|Newer Volcanic Group|50157|5|Briefly described|Map Legend|Pleistocene|Miocene|Lava flows: olivine basalt, tholeiitic; moderately to well vesiculated.||||||03-FEB-09
38291|Newer Volcanic Group|50158|5|Briefly described|Map Legend|Pleistocene|Miocene|Lava flows: olivine basalt, tholeiitic; moderately to well vesiculated.||||||03-FEB-09
38291|Newer Volcanic Group|50159|5|Briefly described|Map Legend|Pleistocene|Miocene|Lava flows: olivine basalt, tholeiitic; moderately to well vesiculated.||||||03-FEB-09
38291|Newer Volcanic Group|50160|5|Briefly described|Map Legend|Pleistocene|Miocene|||||||16-JUN-04
38291|Newer Volcanic Group|50161|5|Briefly described|Map Legend|Pleistocene|Miocene|Lava Flows.||||||26-AUG-04
38291|Newer Volcanic Group|50162|5|Briefly described|Map Legend|Pleistocene|Miocene|Lava flows: olivine basalt, tholeiitic; moderately to well vesiculated.||||||03-FEB-09
38291|Newer Volcanic Group|50163|5|Briefly described|Map Legend|Pleistocene|Miocene|Lava flows: olivine basalt, tholeiitic; moderately to well vesiculated.||||||03-FEB-09
38291|Newer Volcanic Group|62370|5|Briefly described|p447|Holocene|Miocene|Includes all basaltic flows in the Central Highlands palaeovalleys region - infilling deep-lead palaeochannels. Lavas are fine-grained, moderately weathered, variably vesicular black to grey olivine basalt. Age: 7.0Ma to Holocene era. See Newer Volcanics.||||||09-JUN-06
38291|Newer Volcanic Group|64612|2|Defined|p31, p40, p47, p48, p49-52, -72|Early Pliocene|Miocene|Overlies Castlemaine Supergroup, Heathcote Volcanic Group and Murrindindi Supergroup via angular unconformity. Overlies disconformable, Bacchus Marsh Formation. Age: 5.57+/-0.06 and 4.82+/- 0.05Ma. Thickness: 100m. Tholeiitic olivine basalt.||||||03-JUL-13
38291|Newer Volcanic Group|64619|5|Briefly described|Map legend|Pliocene|Miocene|Includes Smokers Creek Volcanic Subgroup and unnamed sheetflow basalt, unnamed scoria deposits and unnamed lavas.||||||
38291|Newer Volcanic Group|64769|6|Mentioned|p26|Cenozoic|Cenozoic|Age: 5 to 0.1Ma. Alkalic to mainly tholeiitic composition. VIC.||||||06-MAY-09
38291|Newer Volcanic Group|65715|4|Described|p17-18, p110||Tortonian|Includes Smokers Creek Volcanic Subgroup. Overlies Werribee Formation. Overlain by Darley Gravel, Deutgam Silt. <10 Ma predominantly basaltic volcanic rocks with minor intermediate and felsic volcanic rocks, as well as minor dykes, plugs and sills.||||||
38291|Newer Volcanic Group|65969|6|Mentioned|p17 Fig.7|||||||||
38291|Newer Volcanic Group|66002|5|Briefly described|p12, p13 Tb.9, p18|Neogene|Neogene|Includes Tower Hill Tuff. Of Krause 1874. Defined VandenBerg 2009. Also referred to as Newer Volcanic rocks (p12). Replaces Newer Volcanics||||||
38291|Newer Volcanic Group|66012|4|Described|p4, p6, p7-8, p9-10 Tb.1, p13-21, p23|Pleistocene|Pliocene|Unconformably overlies Pyrenees Formation and disconformably overlies Lismore Granodiorite. Interfingers with Moorabool Viaduct Sand. Several unnamed units recognised. Tholeiitic to strongly alkaline. Late Pliocene to Pleistocene| | ||||13-JUN-13
38291|Newer Volcanic Group|66244|5|Briefly described|p7.|||Includes units <10 Ma, eg the Hildene Basalt of Edwards et al. (1997).||||||
38291|Newer Volcanic Group|66769|6|Mentioned|121|Late Pliocene|Late Pliocene|Contains c.580 Ma charnockitic xenoliths, suggesting the Selwyn Block basement is continuous with Proterozoic rocks on King Island and Tasmania.||||||
38291|Newer Volcanic Group|68116|5|Briefly described|Maps 23-25, 30-33, 38-42, 47-50.|Holocene|Miocene|Also occurs in the Appendix. Informally subdivided into alkaline, basalt, icelandite, scoria, stony, trachyte, tuff rings, and valley-filling basalt divisions.|||||Mafic to lesser intermediate and ultramafic lavas and pyroclastics and minor intrusive rocks, interbedded sedimentary rocks.|
38291|Newer Volcanic Group|68189|6|Mentioned|p15 Fig.6, p17 Fig.7, pp30-32|||Exhibits high frequency magnetic responses.||||||
38291|Newer Volcanic Group|70877|5|Briefly described|p13|||Referred to mistakenly as the Newer Volcanics on p41.|||||Basaltic lava flows.|
38291|Newer Volcanic Group|70967|6|Mentioned|p3, 11, 17, 20, 28|Cenozoic|Cenozoic||||||Thin basalt lava flows.|
38291|Newer Volcanic Group|71593|4|Described|p55-56, p44-p45, p47|Holocene|Miocene|Covers up to 15000km ^2 in western victoria. Interpreted as a large intraplate basalt province. Thickness is typically tens of metres. Basalt goechemistry is between alkali Appears as the Newer Volcanics on p45 and p138. See also p8-p9, p12, p60, p102, p133, p198, p203.|2-4 Ma (Gray and McDougall, 2009) in area.|||Unconformably overlies the Rocklands Volcanic Group.|Intraplate basaltic lavas developed as sheet and valley-fill flows.|17-SEP-18
38291|Newer Volcanic Group|72445|5|Briefly described|p2, p10, p16, p19; App.1; App.2; App.5|Pliocene|Pliocene|Murray and Otway basins. Part of the cover rocks in the Stavely Project area. Massive to highly vesicular basalt. Aproximately 30cm interflow gravel/soil interval developed at 13.9 m in Stavely01.||||Unconformably overlies Wunghnu Group.|Massive to highly vesicular basalt. C. 30 cm interflow gravel/soil interval developed at 13.9 m in Stavely01.|15-OCT-20
38291|Newer Volcanic Group|73497|5|Briefly described|Map legend|Holocene|Holocene||||||Lava flows, minor scoria: high frequency, moderately reversely magnetised responses (-85 nT); low K, Th and U.|
27521|Ngankipari Sand|22525|6|Mentioned|p37.41||Holocene|||||||
27521|Ngankipari Sand|23489|4|Described|p47|Pleistocene|Pleistocene|||||||
27521|Ngankipari Sand|36127|6|Mentioned|p7|||||||||
27521|Ngankipari Sand|38290|6|Mentioned|p46|||||||||
27521|Ngankipari Sand|39351|6|Mentioned|Map legend|Quaternary|Quaternary|||||||
27521|Ngankipari Sand|41551|5|Briefly described|p464|||||||||
27521|Ngankipari Sand|44198|2|Defined|p48|Holocene|Holocene|||||||
27521|Ngankipari Sand|44199|2|Defined|p594,596,597, 601|Quaternary|Neogene|late Tertiary - Quaternary. Alluvial, derived from source now below sea to W.||||||
27521|Ngankipari Sand|44200|6|Mentioned|p.352, 355.|||||||||
27521|Ngankipari Sand|70660|5|Briefly described|p10|Holocene|Holocene|||||||
27521|Ngankipari Sand|72450|5|Briefly described|Brochure map||||||||Weakly cemented, wind-blown sand.|
27521|Ngankipari Sand|73236|4|Described|p36-38, p43|Late Pleistocene|Late Pleistocene|Wind-blown sediments. Defined by Ward (1966) from near the Hallett Cove Beach railway station.||||Underlain by Pooraka Formation.|Pale orange-brown, medium-grained well-rounded sand; weakly consolidated and penetrated by calcrete.|
29909|Ngarinya Adamellite|24496|5|Briefly described|p16|Mesoproterozoic|Mesoproterozoic|Age: 1186+/-10 Ma (Maboko et al., 1991). Of the Kulgera Suite. Geological Province: Musgrave Block.||||||04-FEB-05
29909|Ngarinya Adamellite|43052|5|Briefly described|p162|||of Kulgera Suite||||||
29909|Ngarinya Adamellite|50607|5|Briefly described|p2.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Musgrave Block. Of the Kulgera Supersuite. Age: 1186 +/- 10Ma (U-Pb).||||||
29909|Ngarinya Adamellite|61154|6|Mentioned|p42 Appendix|||of the Pitjantjatjara Supersuite in South Australia.||||||
28251|Nildottie Siltstone Member|35835|2|Defined|p207|Middle Cambrian|Early Cambrian|Lower to Middle Cambrian||||||
28251|Nildottie Siltstone Member|35954|6|Mentioned|p1229|||See also Fig.2.||||||
28251|Nildottie Siltstone Member|36495|6|Mentioned|p129|||||||||
28251|Nildottie Siltstone Member|37326|6|Mentioned|p3|||||||||
28251|Nildottie Siltstone Member|37802|4|Described|p71|||||||||
28251|Nildottie Siltstone Member|42269|6|Mentioned|p335|||||||||
28251|Nildottie Siltstone Member|44133|4|Described|p27, 28|||Of the Billy Creek Formation. Maximum Thickness: 460m. Disconformably overlies: lower Wilkawillina Limestone.||||||
28251|Nildottie Siltstone Member|60959|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of the Billy Creek Formation. Ripple laminated, coarse-grained greyish-red siltstone with minor shale and fine-grained sandstone.||||||
28251|Nildottie Siltstone Member|68735|6|Mentioned|p238|||||Of the Billy Creek Formation.||||
27650|Nilgenee Member|23719|4|Described|p23|Mesoproterozoic|Mesoproterozoic|See also page 22 table 5. Of Corunna Conglomerate. Overlying unit Cowleds Member. Geological Province: Gawler Craton. Max. thickness 800 m.||||||
27650|Nilgenee Member|37621|6|Mentioned|p15|||||||||
27650|Nilgenee Member|39349|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
27650|Nilgenee Member|40448|6|Mentioned|p36|||||||||
27650|Nilgenee Member|71235|6|Mentioned|p8-p9|||Probably shallow marine in origin.||Corunna Conglomerate||Intertongues with the Cowleds Member.|Sandstone.|
27650|Nilgenee Member|73103|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|||Corunna Conglomerate.|||Sandstone, heavy mineral rich, with minor red siltstone.|
69798|Ninnerie Supersuite|62592|5|Briefly described|p12, p13, p18, p34, p43. |Calymmian|Calymmian|New name. Result of late-Olarian Orogeny crustal melting; voluminous S-type granites: sharply-defined stocks intruding the Strathearn Group, but diffused by migmatites in lower parts.|1595 - 1580 Ma.||Includes Bimbowrie and Crockers Well Suites and Benagerie Volcanics.|Intrudes Strathearn Group.|Granites and volcanics; biotite(-muscovite) granites with a small component of mantle-derived material.|
69798|Ninnerie Supersuite|62993|5|Briefly described|p24|Paleoproterozoic|Paleoproterozoic||||Includes Bimbowrie Suite.|||17-DEC-21
69798|Ninnerie Supersuite|63866|5|Briefly described|p42||||||Includes the Bimbowrie Suite.||Syn- to post-orogenic granites.|
69798|Ninnerie Supersuite|64741|5|Briefly described|p313|||Includes Bimbowrie Suite and Crockers Well Suite. Dominantly felsic intrusives. S-types. Granites not foliated except near late shear zones|Age ranges: ~1590-1580Ma|||||07-FEB-11
69798|Ninnerie Supersuite|66302|5|Briefly described|p50, p51, p69, p75|||Olary Domain, Curnamona Province. |||Includes the Bimbowrie Suite and Crocker Well Suite||A, I and S type granites.|
69798|Ninnerie Supersuite|66518|5|Briefly described|p19 Fig.4.|Mesoproterozoic|Mesoproterozoic|Curnamona Province.|c.1590 Ma.||Includes Crocker Well Suite and Honeymoon Type granite.|||
69798|Ninnerie Supersuite|66575|6|Mentioned|p948,|||Curnamona Province. Experienced felsic activity c.1600 Ma.||||||
69798|Ninnerie Supersuite|67540|2|Defined|pp25-42|Calymmian|Statherian|Named after Ninnerie Hill. To include all early Mesoproterozoic magmatic rocks that developed in the Curnamona Province between 1600-1570 Ma (Cook et al. 1994; Jagodzinski and Fricke 2010; Page et al. in prep.); the intrusions into Willyama Supergroup and Radium Creek Metamorphics, and the volcanics extruded onto Willyama Supergroup metasediments. Comprises 4 Suites, 9 Formations, 5 unassigned units and 3 unnamed subunits. Includes Benagerie 1 (Wittakilla) and Benagerie 2 (Qunyambie), Ninnerie 1, and the undefined granites in the Broken Hill and Mulyungarie domains. Previously Bimbowrie Supersuite (Conor et al. 2006).|~1600-1570 Ma ||Includes Benagerie Volcanic, Bimbowrie, Crocker Well and Coulthard Suites; Windamerta Diorite, Billeroo Intrusive Complex, Honeymoon Granite, Lake Charles Diorite and Pepegoona Porphyry.|Overlies the Willyama Supergroup.|Ranges from felsic S-type granites to intermediate and alkaline I-type granites, and A-type felsic and mafic volcanics; generally enriched in REE and HFSE.|
69798|Ninnerie Supersuite|67581|6|Mentioned|p44 Fig.8|||Curnamona Province.|1600-1555 Ma.|||||
69798|Ninnerie Supersuite|67900|5|Briefly described|p18, 20, 32|Mesoproterozoic|Mesoproterozoic|Curnamona Province. Appears to have formed mostly from partial melting of Willyama Supergroup and lower crust.|||Bimbowrie, Crocker Well, Coulthard, Benagerie Volcanic, Suites.|Intrudes Willyama Supergroup.|Vast quantities of S- and I-type granites and A-type volcanic rocks.|
69798|Ninnerie Supersuite|68126|5|Briefly described|p1, p3, p5-8, p12, p15-16, p29-30|Mesoproterozoic|Mesoproterozoic|Fricke (2006, 2008), for late- to post-Olarian Orogeny igneous intrusive and extrusive rocks in the Curnamona Province.|1600-1570 Ma.||Bimbowrie, Crocker Well Suites; Honeymoon Granite, Benagerie Volcanics.||Monzogranite, trondhjemite, granodiorite to diorite, rhyolite to trachyte, basalt; sandstone interbeds.|
69798|Ninnerie Supersuite|69019|6|Mentioned|p172 Fig.40.|Mesoproterozoic|Mesoproterozoic|At depth of c.4000m, underlies Adelaide Geosyncline rocks below Cambrian Arrowie Basin and Mesozoic Eromanga Basin sediments.||||||
69798|Ninnerie Supersuite|69562|5|Briefly described|p670-672 Tb.5, p674 Fig.6||||1590-1550 Ma.||Includes Basso and Bimbowrie Suites and Honeymoon Granite.||Includes fine-grained basalt.|
69798|Ninnerie Supersuite|69650|2|Defined|p1- 75|Mesoproterozoic|Mesoproterozoic|Curnamona Province. Named after Ninnerie Hill. Previously Bimbowrie Supersuite (Conor et al., 2006). Crustal sedimentary source (Willyama Supergroup  metasediments) except mafic volcanics derived from more juvenile mantle sources. Distribution (on maps) listed. Also includes 3 un-named units.|||Includes Bimbowrie, Crocker Well, Benagerie Volcanic, Coulthard Suites; Pepegoona Porphyry; Lake Charles, Windamerta Diorites; Honeymoon Granite; Billeroo Intrusive Complex.|Granites intrude, volcanics overlie Willyama Supergroup. Intrudes Radium Creek Metamorphics.|Felsic S-type to intermediate I-type and alkaline granites; A-type felsic and mafic volcanics.|08-FEB-16
69798|Ninnerie Supersuite|69654|6|Mentioned|p23|Mesoproterozoic|Mesoproterozoic||||Bimbowrie Suite.|||
69798|Ninnerie Supersuite|70339|5|Briefly described|map legend|Mesoproterozoic|Mesoproterozoic||U-Pb age 1600 Ma||||Monzogranite, biotite-muscovite; trondhjemite, monzogranite, adamellite and alaskite, biotite-bearing, sodic; granodiorite to diorite; rhyolite to trachyte, porphyritic; basalt, amygdaloidal, hyaloclastic, pillowed sandstone interbeds.|
69798|Ninnerie Supersuite|70340|5|Briefly described|map legend|Mesoproterozoic|Mesoproterozoic||U-Pb age 1600 Ma||||Monzogranite, muscovite-biotite; trondhjemite, monzogranite, adamellite and alaskite, biotite-bearing, sodic; granodiorite to diorite; rhyolite to trachyte, porphyritic; basalt, amygdaloidal, hyaloclastic, pillowed, sandstone interbeds.|
69798|Ninnerie Supersuite|70384|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic||||Coulthard Suite, Pepegoona Porphyry.||Granite, porphyry, trondhjemite, granitic gneiss, silicic metavolcanic rock, crystal tuff, rhyolite.|
69798|Ninnerie Supersuite|70405|5|Briefly described|p1 ,p9 table 1, p12 figure 4, p44, p97|Mesoproterozoic|Mesoproterozoic|Includes undeformed leucogranite dykes that are aged at 1560 Ma.|1590 Ma -1580 Ma||Includes Bimbowrie Suite, Crocker Well Suite, Windamerta Suite||Felsic magmatic units (granitoids).|
69798|Ninnerie Supersuite|70657|4|Described|p13 Fig.6, p25, p45, p48-50, p54, p56-59|Calymmian|Calymmian|See also p61-62, p66. Olary, Mulyungarie, Broken Hill Domains, Curnamona Province. New name; proposed in this study to include all the Mesoproterozoic granites in the region, as well as the syn- to post-tectonic granites of the Broken Hill Domain. Some granites are surrounded by aureoles of Morialpa Migmatite. Non-foliated to weakly foliated. At least in part the product of anatexis (late Olarian Orogeny). Forms prominent, large dome-shaped outcrops. Temporal relationship with Hiltaba Suite / Gawler Range Volcanics. Mineralisation (U, Th, REE) described.|1595-1575 Ma|In Willyama Supergroup.|Mundi Mundi Granite.|In Willyama Supergroup.|Voluminous syn- to post-orogenic, S-type-dominated granites. Relatively leucocratic, white to pale pink, equigranular to locally strongly porphyritic, biotite- or biotite-muscovite-monzogranites|
69798|Ninnerie Supersuite|70658|5|Briefly described|p2, 4, 10, 29, 32-34|Mesoproterozoic|Mesoproterozoic|Curnamona Province. Late-stage Olarian Orogeny.|c.1594 - c.1570 Ma.||Coulthard, Benagerie Volcanic, Crocker Well, Bimbowrie, Suites.||Granites.|
69798|Ninnerie Supersuite|70659|5|Briefly described|p2|Mesoproterozoic|Mesoproterozoic|Curnomona Province. Associated with Benagerie Volcanic Suite.|1600-1570 Ma||||Granites.|
69798|Ninnerie Supersuite|70816|5|Briefly described|p4|Calymmian|Statherian|Geological province: Curnamona Province.|1600-1570 Ma|||Plutonic rocks associated with the Benagerie Volcanic Suite.||
69798|Ninnerie Supersuite|70829|6|Mentioned|p28, 31|Mesoproterozoic|Mesoproterozoic|Curnamona Province. Associated with the late stages of the 1620-1585 Ma Olarian Orogeny.|||Benagerie Volcanics.||Granites, mainly S-type.|
69798|Ninnerie Supersuite|70947|6|Mentioned|p960|Calymmian|Calymmian|Geological province: Curnamona Province.|ca. 1580 Ma|||||
69798|Ninnerie Supersuite|71043|6|Mentioned|p104|Calymmian|Calymmian|Gawler Craton.|c.1580 Ma.|||||
69798|Ninnerie Supersuite|71317|6|Mentioned|p20|||Curnamona Province.||||||
69798|Ninnerie Supersuite|71341|6|Mentioned|p179 fig 1|Mesoproterozoic|Palaeoproterozoic||ca. 1600-1570 Ma|||||
69798|Ninnerie Supersuite|72454|5|Briefly described|p1-p3, p2 Fig.2, p11|Mesoproterozoic|Mesoproterozoic|Curnamona Province. See also p20, p22, p25, p39, p49-55. Granites from this supersuite can be found in the Olary Domain, Mudguard Domain, Mulyungarie Domain and the Broken Hill Domain.|c. 1500 to 1570 Ma.||Includes Bimbowrie Suite, Crocker Well Suite, and an unnamed suite of granodiorites to diorites, in Olary Domain.||Includes granites, granodiorites, diorites.|
69798|Ninnerie Supersuite|72462|6|Mentioned|p1-2, p5, p7|Calymmian|Calymmian|Curnamona Province. Part of a silicic large igneous province; originally contiguous with the Gawler Range Volcanics and Hiltaba Suite.|1600-1570 Ma|||||
69798|Ninnerie Supersuite|72949|6|Mentioned|p34||||ca. 1.58 Ga|||||
69798|Ninnerie Supersuite|73030|6|Mentioned|p2148, p2150, p2153|Calymmian|Calymmian|Curnamona Province. Associated with the Benagerie Volcanic Suite.|ca. 1580 Ma|||||
69798|Ninnerie Supersuite|73155|6|Mentioned|p264 Fig.1|Calymmian|Calymmian|Curnamona Province.|ca. 1580 Ma||||Intrusives.|
69798|Ninnerie Supersuite|73162|6|Mentioned|p448, p449|Mesoproterozoic|Mesoproterozoic|Curnamona Province.|1600-1570 Ma|||||
69798|Ninnerie Supersuite|73165|6|Mentioned|p637, Fig. 12, p638|||Curnamona Province. Intruded synchronously with, and immediately following deformation events, emplaced during the generation of later upright folds. Suggested to be temporal equivalents of the 1595-1575 Ma Hiltaba Suite, although of different composition.|ca 1600-1575 Ma||||Granites.|
69798|Ninnerie Supersuite|73235|6|Mentioned|p52|Calymmian|Calymmian||c. 1580 Ma|||||
69798|Ninnerie Supersuite|73251|6|Mentioned|p36-37|Calymmian|Calymmian|Curnamona Province. Includes uraniferous crystalline rock. Inferred source of paleochannel-hosted uranium.|c. 1590 Ma||Crocker Well Suite, Honeymoon Granite|||
69798|Ninnerie Supersuite|73429|6|Mentioned|p105, p107, p110, p114|Calymmian|Calymmian|Curnamona Province, central.|~1600-1580 Ma||||Granites.|
69798|Ninnerie Supersuite|73516|5|Briefly described|p2, p3 Fig.1, p6-7|Calymmian|Calymmian|Curnamona Province. S- and I-type. Approximately aligned with the Curnamona Conductor in magnetotelluric data. [also written as including A-type Hiltaba granites p6].|1600-1550 Ma|||Intrudes Willyama Supergroup|Granites.|
69798|Ninnerie Supersuite|73524|6|Mentioned|p4, p20|Calymmian|Calymmian|Curnamona Province. S-type granitic magmatism. Thought to be derived from partial melting of structurally lower portions of Willyama Supergroup, intrudes into its higher portions. Correlative of Hiltaba Suite.|c. 1600-1570 Ma|||Intrudes Willyama Supergroup||
69798|Ninnerie Supersuite|74367|6|Mentioned|p23|||Curnamona Province.||||||
73299|Nirranda Supersequence|63134|2|Defined|111-112|||||||||
73299|Nirranda Supersequence|63269|5|Briefly described|p605|Oligocene|Eocene|Otway Basin.||||Overlies Wangerrip Supersequence. Is overlain by Heytesbury Supersequence.||
73299|Nirranda Supersequence|69297|6|Mentioned|p80, p98, p110, p111|||Misspelt as the Nirrandra Supersequence on p98. ||||||
73299|Nirranda Supersequence|69651|5|Briefly described|p10, p12-15, p17-19, p22-23, p29, p39|Oligocene|Eocene|See also p44-47, p49-50. Relatively thin and undeformed open marine deposits; marks a major marine transgression. Possible seals. Modelling diagrams.||||Overlies Wangerrip Supersequence conformably [!]. Is overlain by Heytesbury Supersequence.|Calcareous claystone overlain by marls, calcarenite and calcilutite; shaly limestone overlain by calcarenite and calcilutite; quartz sandstone overlain by silty mudstone, and limestone.|
73299|Nirranda Supersequence|70077|5|Briefly described|Regional: Fig.4; p4-5|Oligocene|Eocene|Otway Basin.||||Overlies Wangerrip Supersequence. Is overlain by Heytesbury Supersequence.||
73299|Nirranda Supersequence|70078|5|Briefly described|Regional: Fig.4; p3|Oligocene|Eocene|Deposition was truncated by a major mid-Oligocene unconformity.||||Overlies Wangerrip Supersequence. Is overlain unconformably by Heytesbury Supersequence.|Shallow-marine sandstones, marls and limestones.|
73299|Nirranda Supersequence|70880|5|Briefly described|p77|Oligocene|Eocene|Otway Basin. Open marine environment.||||Overlies Wangerrip Supersequence. Is overlain by Heytesbury Supersequence.|Mixed carbonate/siliciclastic sediments.|
73299|Nirranda Supersequence|71266|5|Briefly described|p614 Fig.3, p615|Oligocene|Eocene|Otway Basin.||||Overlies Wangerrip Supersequence. Is overlain by Heytesbury Supersequence.||
79743|Nonning Rhyolite Member|70659|5|Briefly described|p8|||Gawler Ranges.||Eucarro Rhyolite.||||
79743|Nonning Rhyolite Member|70816|5|Briefly described|p5|||Gawler Ranges region.||Unit of Eucarro Rhyolite||Overlain by Paney and Yannabie Rhyolite Members. Underlain by an black or brown base of flow as the base of the Eucarro Rhyolite.||
79743|Nonning Rhyolite Member|72090|6|Mentioned|p12|||Gawler Craton.||Eucarro Rhyolite||||
79743|Nonning Rhyolite Member|73110|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|||Eucarro Rhyolite.|||Rhyolite, massive, red to pink, columnar jointed, with scattered granitoid and lithic megacryst-bearing clasts.|
23877|Nooldoonooldoona Trondhjemite|22631|6|Mentioned|p176|Calymmian|Calymmian|||||||
23877|Nooldoonooldoona Trondhjemite|23775|5|Briefly described|p721||Mesoproterozoic|||||||22-SEP-09
23877|Nooldoonooldoona Trondhjemite|42885|2|Defined|p20||Mesoproterozoic|see also Fig.2 p22. Type area: North along the ridgetop road track from Coulthards Lookout (Fig. 2), a well-known tourist viewing area.||||||25-NOV-22
23877|Nooldoonooldoona Trondhjemite|43052|5|Briefly described|Table 5.12|||||||||
23877|Nooldoonooldoona Trondhjemite|50605|5|Briefly described|p10.2|||Of the Babbage Supersuite. Geological Province: Gawler Craton & Curnamona Province.||||||
23877|Nooldoonooldoona Trondhjemite|67540|3|Fully described|p25, p27-28, p36 Tb.3, p40 Fig.2|Calymmian|Calymmian|Named after Nooldoonooldoona Waterhole. Type locality: Ridge Top Track 500 m N of Coulthards Lookout. Curnamona Province: Moolawatana Domain. Definition reference: Coats and Blissett (1971), this article, and Fricke and Hore (2011). Age determined using Kober zircon Pb/Pb. This unit may well be merely an alteration of the Mount Neill Granite.|1576 +/- 2.4 Ma (Janka et al. 1999).|Of the Coulthard Suite.||Intrudes the Radium Creek Metamorphics.|Grey, pink-weathering, medium- to coarse-grained sodic intrusive with rounded to euhedral albitic plagioclase phenocrysts; rare quartz phenocrysts, bluish and containing fluorine-rich magnesian biotite; granophyric textures are observed. A-type.|08-FEB-16
23877|Nooldoonooldoona Trondhjemite|69562|5|Briefly described|p670 Tb.5|||Na-altered Mount Neill Granite. Magmatic age of precursor. Age of metasomatism ?1555 Ma.|1575 +/- 3 Ma (Edburg et al. 2001).|||||
23877|Nooldoonooldoona Trondhjemite|69650|1|Redefined|p4 Tb.1; p9,p11,p13,p57-61,p65-67,p73|Calymmian|Calymmian|Coats and Blissettt (1971). Named after Nooldoonooldoona Waterhole, near Arkaroola. Moolawatana Domain, Curnamona Province. Type locality:is found cropping out along the Ridge Top Track north of Coulthards Lookout (Teale, 1993a) centred on GDA94, 340140 mE, 6650100 mN, some 500 m from the lookout . Elburg et al. (2001) concluded this unit is the result of strong metasomatic alteration of Mount Neill Granite; this unit may need reclassifying. Kober zircon Pb/Pb age. Geochemistry detailed.|1576 +/- 2.4 Ma (Janka et al., 1999).|Unit in Coulthard Suite.||Intrudes Radium Creek Metamorphics.|Grey, pink-weathering sodic intrusive, medium- to coarse-grained; rounded to euhedral albitic phenocrysts to 50mm, quartz phenocrysts to 10mm with distinct bluish colour; rare F-rich magnesian biotite; some granophyric textured samples. A-type.|25-NOV-22
23877|Nooldoonooldoona Trondhjemite|70384|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic||1572 +/- 6 Ma (SHRIMP U-Pb).|Coulthard Suite.|||Trondhjemite, grey, pink-weathering, medium- to coarse-grained, albitic plagioclase and bluish quartz phenocrysts; rare fluorite-rich magnesian biotite, local granophyric textures. A-type.|
23877|Nooldoonooldoona Trondhjemite|70658|5|Briefly described|p33-35, 37|Mesoproterozoic|Mesoproterozoic|Curnamona Province. Outcrop area ~6 km2, W from Radium Creek.|1576 +/- 2.4 Ma.|Coulthard Suite.|||Grey, medium- to coarse-grained with rounded through to euhedral albitic plagioclase phenocrysts. Distinct bluish quartz. A-type.|
23877|Nooldoonooldoona Trondhjemite|72454|6|Mentioned|p34, p47|Mesoproterozoic|Mesoproterozoic|Part of Mount Painter Inlier.|||||Includes trondhjemite.|
23877|Nooldoonooldoona Trondhjemite|72459|6|Mentioned|p59-61|Mesoproterozoic|Mesoproterozoic|Previously interpreted as magmatic in origin and intrusive to older gneisses. However work investigating chemistry of this unit shows it may instead represent metasomatised Mt Neill Suite rather than a separate magmatic unit.|1576 +/- 2.4 Ma (U-Pb zircon; Janka et al, 1999)|Mt Neill Suite||||
26318|Noranda Volcanics|24175|3|Fully described|p8|Neoproterozoic|Neoproterozoic|Of Arkaroola Subgroup. Type section: near Boorloo Mine.||||||13-FEB-08
26318|Noranda Volcanics|24321|5|Briefly described|Map legend|Adelaidean|Adelaidean|Parent: Arkaroola Subgroup||||||
26318|Noranda Volcanics|37854|2|Defined|p9|Adelaidean|Adelaidean|Early Willouran.||||||13-FEB-08
26318|Noranda Volcanics|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Willouran.||||||13-FEB-08
26318|Noranda Volcanics|40294|6|Mentioned|p9|||||||||
26318|Noranda Volcanics|41403|4|Described|p53|||||||||
26318|Noranda Volcanics|42087|5|Briefly described|Fig.2 P15|||||||||
26318|Noranda Volcanics|42222|5|Briefly described|p11|||||||||
26318|Noranda Volcanics|42223|4|Described|p34|||See also Table 1||||||
26318|Noranda Volcanics|42238|5|Briefly described|p71|||||||||
26318|Noranda Volcanics|43052|5|Briefly described|p172,Table 6.1|||Of Arkaroola Subgroup.||||||13-FEB-08
26318|Noranda Volcanics|60718|5|Briefly described|p49 Fig. 2|Adelaidean|Adelaidean|Geological Province: Adelaide Geosyncline. See also p53.||Of Arkaroola Subgroup (Callanna Group) or correlated with it?||||15-APR-11
26318|Noranda Volcanics|64796|6|Mentioned|p190 Fig.8|||||||Is overlain by Dome Sandstone (Curdimurka Subgroup).||
26318|Noranda Volcanics|69666|6|Mentioned|p24, p26, p36|Neoproterozoic|Neoproterozoic|Willouran Ranges. Part of the Willouran Basic Province.||||||
26318|Noranda Volcanics|71129|5|Briefly described|p103|Tonian|Tonian|Geological Province: Gawler Craton. Of Adelaide Geosycline. Part of the Willouran Basic Province, which also includes Beda Basalt, and the Wooltana and Cadlareena volcanics, Wilangee Basalt, Little Broken Hill Gabbro and Gairdner Dolerite. Related to the Rodinian break-up (Zhao et al., 1994, Li et al., 1999, Wang et al., 2010). Basaltic volcanism interpreted to be result of mantle plume upwelling, causing doming in the continental lithosphere (Zhao et al., 1994).||||||
26318|Noranda Volcanics|73222|6|Mentioned|p7|Tonian|Tonian|Adelaide Rift Complex, Willouran Ranges. Willouran.||Arkaroola Subgroup, Callanna Group, Warrina Supergroup||Unconformably underlain by Black Knob Marble. Overlain by Dome Sandstone (Curdimurka Subgroup). Possibly equivalent to Wooltana Volcanics.||
26318|Noranda Volcanics|74367|6|Mentioned|p18, p20|||Willouran Basic Province. Suggested to be coeval with Gairdner Dolerite (827+/-6 Ma, Wingate et al., 1998).||||Correlated with Wooltana Volcanics||
26810|North Maslin Sand|22525|5|Briefly described|p35,37||Eocene|||||||
26810|North Maslin Sand|22528|4|Described|p42-44 Figs 2-6||Middle Eocene|||||||
26810|North Maslin Sand|22541|4|Described|p 19, Fig 1||Middle Eocene|||||||
26810|North Maslin Sand|22587|6|Mentioned|p79 Fig.7|Middle Eocene|Middle Eocene|||||||
26810|North Maslin Sand|23482|5|Briefly described|p10|Middle Eocene|Middle Eocene|||||||
26810|North Maslin Sand|23489|4|Described|p43|Oligocene|Eocene|North Maslin Sand and South Maslin Sand are known collectively as Maslin sands (informal).||||||
26810|North Maslin Sand|23731|6|Mentioned|p29|Middle Eocene|Middle Eocene|||||||
26810|North Maslin Sand|23802|5|Briefly described|p21 Fig. 2|||Unconsolidated sand.||||||
26810|North Maslin Sand|41025|6|Mentioned|Fig.2|||||||||
26810|North Maslin Sand|41513|6|Mentioned|p40|||||||||
26810|North Maslin Sand|41515|6|Mentioned|p116|||||||||
26810|North Maslin Sand|41520|6|Mentioned|Fig.2|||||||||
26810|North Maslin Sand|41626|6|Mentioned|p56|||||||||
26810|North Maslin Sand|42099|6|Mentioned|p68|||||||||
26810|North Maslin Sand|42498|5|Briefly described|Map Legend|Eocene|Eocene|||||||
26810|North Maslin Sand|42506|5|Briefly described|Map legend|Eocene||Age Tertiary||||||
26810|North Maslin Sand|43052|5|Briefly described|Table 2.1|||||||||
26810|North Maslin Sand|43053|5|Briefly described|Map Legend|Eocene|Paleocene|Fluvial to marginal marine siliceous sand. Geological Province: St Vincent Basin.||||||25-MAY-05
26810|North Maslin Sand|43258|5|Briefly described|Map Legend|Eocene|Paleocene|||||||
26810|North Maslin Sand|43298|5|Briefly described|Map Legend|Eocene|Paleocene|||||||
26810|North Maslin Sand|44133|5|Briefly described|p164, 152 Fig. 10.2|Middle Eocene|Middle Eocene|Formerly North Maslin Sands. Geological Province: Saint Vincent Basin.||||||
26810|North Maslin Sand|44198|5|Briefly described|p16|Miocene|Eocene|||||||
26810|North Maslin Sand|60538|5|Briefly described|p479 Fig. 18|Oligocene|Eocene|Geological Province: Saint Vincent Basin.||||||
26810|North Maslin Sand|60953|5|Briefly described|Map Legend|Eocene|Paleocene|Fluvial to marginal marine siliceous sand. Geological Province: Saint Vincent Basin.||||||27-APR-05
26810|North Maslin Sand|60958|5|Briefly described|Map Legend|Eocene|Eocene|Geological Province: Saint Vincent Basin. Cross-bedded fluvial sandstone, conglomerate with minor sandy siltstone, unconsolidated.||||||14-APR-05
26810|North Maslin Sand|61108|5|Briefly described|map legend|Eocene|Paleocene|Fluvial to marginal marine siliceous sand. Geological Province: St Vincent Basin.||||||
26810|North Maslin Sand|61121|5|Briefly described|Map legend|Eocene|Eocene|Cross-bedded fluvial sandstone, conglomerate with minor silty sandstone, unconsolidated. Unfossiliferous. Age is possible Middle Eocene.||||||
26810|North Maslin Sand|61837|5|Briefly described|p216|Middle Eocene|Middle Eocene|Fluvio-lacustrine deposits.||||||
26810|North Maslin Sand|64397|5|Briefly described|p233 Fig. 2|Middle Miocene|Middle Miocene|Cross-bedded quartz sand, with clay lenses and terrestrial flora in lower section. Geological province: St Vincent Basin. Grouped together with South Maslin Sand as the informal Maslin Sands in Fig. 1, p232.||||||
26810|North Maslin Sand|65375|4|Described|pp33-34, p55. |Eocene|Eocene|Paleocurrent analysis suggests east-southeast stream transport. Thickness varies locally up to 60m. Extracted in Price area and north of Melton for concrete or building sand. Age given as Tertiary, but likely to be Middle Eocene.||||Unconformably overlies Kulpara Formation. Is unconformably overlain by Hindmarsh Clay.|Cross-bedded fluvial sand and gravel.|
26810|North Maslin Sand|65891|6|Mentioned|p221 Fig.5, p222 Fig.7, p228 Fig.11.|Paleogene|Paleogene|Eastern St Vincent Basin. Age shown as Lutetian to Bartonian.||||||
26810|North Maslin Sand|66131|6|Mentioned|p242 Fig.2|Eocene|Eocene|Middle Eocene in Age (from p.242 Fig.2 - stratigraphic correlation chart).||||||
26810|North Maslin Sand|66194|5|Briefly described|p581-p582, p585, 592,593|Eocene|Eocene|Middle Eocene; homogeneous massive sandy sediment with occasional bands of quartz and ferruginous clasts. In St Vincent Basin. High energy river deposit.||||||28-MAR-13
26810|North Maslin Sand|67462|5|Briefly described|Map legend.|Eocene|Eocene|Saint Vincent Basin.||||||
26810|North Maslin Sand|68715|6|Mentioned|p31 Fig.5|Lutetian|Ypresian|St Vincent Basin.||||||
26810|North Maslin Sand|70660|4|Described|p3, p9-p14, p22|Bartonian|Lutetian|See also the Maslin Sand. This unit was interpreted to have been deposited in braided streams or fluvio-lacustrine environments. Sands of this unit are <30m thick. See also p25-p26, p33, p42-p43, p46.||||Overlies the Cape Jervis Formation and the Burra Group. Overlain by the South Maslin Sand.|Cross-bedded quartz sands and gravels along with ultramature and carbonaceous clays.|
26810|North Maslin Sand|70722|5|Briefly described|p218|Middle Eocene|Middle Eocene|Of St. Vincent Basin. ||||Overlain by South Maslin Sand.||
26810|North Maslin Sand|71789|6|Mentioned|p100|||||||||
26810|North Maslin Sand|72450|5|Briefly described|Brochure, Brochure map|Eocene|Eocene|Deposited in a fluvial setting. Crops out along the northern margin of the Willunga Embayment between Yangarra and Maslin Beach. Exposed in road cuts near Oliver Hill and along Chapel Hill Road.||||Underlies the South Maslin Sand.||
26810|North Maslin Sand|73188|5|Briefly described|[See comments]|Middle Eocene|Middle Eocene|St Vincent Basin and ?Mount Lofty Ranges. Adelaide Plains, northern. Ferruginised disconformity surface between this unit and the South Maslin Sand. Deposited in fluviatile environments. At least locally, the top of this unit was oxidised with ferruginous induration before deposition of the South Maslin Sand. p: 313-314, 318-320, 327-328, 333, 335-337, 345, 349-351, 355-356, 359.||||Disconformably overlain by South Maslin Sand.|Fluvial sand and gravel with black clay lenses.|
26083|Nuckulla Basalt|24474|4|Described|p40|||Of the Glyde Hill Volcanic Complex.  Conformably overlies the Bunburn Dacite.  Geological Province: Gawler Craton.||||||
26083|Nuckulla Basalt|30984|2|Defined|p12|Proterozoic|Proterozoic|||||||
26083|Nuckulla Basalt|41974|5|Briefly described|p411|||||||||
26083|Nuckulla Basalt|42546|5|Briefly described|Map legend|Mesoproterozoic||||||||
26083|Nuckulla Basalt|42722|6|Mentioned|map legend|Carpentarian||Overlies the Bunburn Dacite.||||||07-APR-05
26083|Nuckulla Basalt|42736|5|Briefly described|map legend|Mesoproterozoic||||||||
26083|Nuckulla Basalt|43052|5|Briefly described|p111|||of Glyde Hill Volcanic Complex||||||
26083|Nuckulla Basalt|43071|4|Described|p14,Table 2|||of Gawler Range Volcanics||||||
26083|Nuckulla Basalt|63398|5|Briefly described|p670 Fig. 6d|Mesoproterozoic|Mesoproterozoic|Age: ca 1590Ma. Geological Province: Gawler Craton. ||||||
26083|Nuckulla Basalt|67909|6|Mentioned|p126-127, 130|Mesoproterozoic|Mesoproterozoic|Lake Everard area. Has limited areal and volume extent.||Glyde Hill Volcanic Complex.||||
26083|Nuckulla Basalt|69649|5|Briefly described|p24|Mesoproterozoic|Mesoproterozoic|Giles (1977). Crops out over a limited area near Nuckulla Well and Dam. Overlain by a thin layer of (?volcaniclastic) sediment.||Unit in Glyde Hill Volcanic Complex.||Conformably overlies Bunburn Dacite.|A massive, dark green to grey, phenocryst-poor, fine-grained basaltic lava flow.|26-FEB-15
26083|Nuckulla Basalt|70659|4|Described|p7, p8|Mesoproterozoic|Mesoproterozoic|Limited extent; total thickness 80m.||Glyde Hill Volcanic Complex.||Copnformably overlies Bunburn Dacite.|Massive basaltic lava flows.|06-FEB-17
26083|Nuckulla Basalt|70738|6|Mentioned|p186-187|||Gawler Craton.||Glyde Hill Volcanic Complex.||||
26083|Nuckulla Basalt|70816|5|Briefly described|p5|||Geological province: Lake Everard, Gawler Ranges.||Unit of Glyde Hill Volcanic Complex.||Overlain by Yantea Rhyolite? Underlain by Baldry Rhyolite.||
26083|Nuckulla Basalt|72090|6|Mentioned|p12|||Gawler Craton.||Glyde Hill Volcanic Complex||||
25355|Nullarbor Limestone|22485|5|Briefly described|p51 , Fig 2|Tertiary|Tertiary|||||||
25355|Nullarbor Limestone|22587|6|Mentioned|p79 Fig. 7|Middle Miocene||||||||
25355|Nullarbor Limestone|22814|5|Briefly described|p258, fig2|Tertiary|Tertiary|||||||
25355|Nullarbor Limestone|23488|6|Mentioned|p39|Miocene|Miocene|Geological Province: Eucla Basin.||||||
25355|Nullarbor Limestone|23671|6|Mentioned|p1|||Overlies the Pidinga Formation.||||||
25355|Nullarbor Limestone|23768|5|Briefly described|p28 Fig.5|Middle Miocene|Middle Miocene|Geological Province: Eucla Basin.  See also p19, p185-187.||||||10-MAR-05
25355|Nullarbor Limestone|23818|4|Described|p174 Fig.84, p198|Early Miocene|Early Miocene|Geological Province: Eucla Basin. Underlain by Wilson Bluff Limestone. Max. thickness: 100 ft.||||||14-MAY-07
25355|Nullarbor Limestone|24057|5|Briefly described|p97|Middle Miocene|Middle Miocene|Geological Basin: Eucla Basin.||||||
25355|Nullarbor Limestone|24201|5|Briefly described|p373 Fig. 2|Oligocene|Eocene|||||||
25355|Nullarbor Limestone|24338|5|Briefly described|p938 Fig. 2|Rupelian|Lutetian|Overlies the Pidinga Formation. Geological Province: Bight Basin.||||||
25355|Nullarbor Limestone|24347|5|Briefly described|p114|Middle Miocene|Middle Miocene|Geological Province: Eucla Basin.||||||
25355|Nullarbor Limestone|24350|5|Briefly described|Fig. 4 Appdx|Oligocene|Eocene|Part of the Dugong Supersequence.||||||
25355|Nullarbor Limestone|24396|5|Briefly described|p222 Fig. 5, p228|Early Pliocene|Middle Miocene|Age: 15.5-5Ma.||||||24-FEB-10
25355|Nullarbor Limestone|24553|5|Briefly described|Figs. 7,8 and 10|Recent|Late Eocene|Along with Wilson Bluff Limestone, equivalent to the Dugong Supersequence.||||||21-JAN-16
25355|Nullarbor Limestone|24606|5|Briefly described|p956, p958 Fig. 3|Early Pliocene|Middle Miocene|Geological Province: Eucla Basin||||||
25355|Nullarbor Limestone|29550|6|Mentioned|p44|||Tertiary||||||
25355|Nullarbor Limestone|29591|5|Briefly described|p92|||||||||
25355|Nullarbor Limestone|29856|6|Mentioned|p37|||||||||
25355|Nullarbor Limestone|30012|5|Briefly described|p20|||Mention Table 1.||||||
25355|Nullarbor Limestone|30268|6|Mentioned|p44|||||||||
25355|Nullarbor Limestone|30514|6|Mentioned|p103|||||||||
25355|Nullarbor Limestone|30563|4|Described|p13|||See stratigraphic table on p6.||||||21-JAN-16
25355|Nullarbor Limestone|30564|5|Briefly described|p12|||||||||
25355|Nullarbor Limestone|30807|6|Mentioned|p101|||Suggested map symbol||||||
25355|Nullarbor Limestone|30917|6|Mentioned|p55|||||||||
25355|Nullarbor Limestone|30922|6|Mentioned|Map legend|Miocene|Miocene|||||||
25355|Nullarbor Limestone|30945|6|Mentioned|Map legend|early Miocene|early Miocene|||||||
25355|Nullarbor Limestone|30952|6|Mentioned|Map legend|early Miocene|early Miocene|||||||
25355|Nullarbor Limestone|30953|6|Mentioned|Map legend|early Miocene|early Miocene|||||||
25355|Nullarbor Limestone|30954|6|Mentioned|Map legend|early Miocene|early Miocene|||||||
25355|Nullarbor Limestone|30962|6|Mentioned|Map legend|early Miocene|early Miocene|||||||
25355|Nullarbor Limestone|30967|6|Mentioned|Map legend|early Miocene|early Miocene|||||||
25355|Nullarbor Limestone|30974|6|Mentioned|Map legend|middle Miocene|middle Miocene|||||||
25355|Nullarbor Limestone|30975|6|Mentioned|Map legend|middle Miocene|middle Miocene|||||||
25355|Nullarbor Limestone|30976|6|Mentioned|Map legend|middle Miocene|middle Miocene|||||||
25355|Nullarbor Limestone|31318|5|Briefly described|p166|||L. Miocene||||||
25355|Nullarbor Limestone|31320|6|Mentioned|p55|||||||||
25355|Nullarbor Limestone|31562|5|Briefly described|p13|||||||||
25355|Nullarbor Limestone|31845|6|Mentioned|p6|||||||||
25355|Nullarbor Limestone|31850|4|Described|p37|||Definition summary.||||||21-JAN-16
25355|Nullarbor Limestone|31902|4|Described|Table 1|||Fig.1||||||
25355|Nullarbor Limestone|31903|6|Mentioned|Map legend|early Miocene|early Miocene|||||||
25355|Nullarbor Limestone|31904|4|Described|p8|||See also Table 1. Refers previous authors||||||
25355|Nullarbor Limestone|31906|4|Described|p8|||Refers previous authors. Table 1||||||
25355|Nullarbor Limestone|31907|4|Described|Table 1|||See also p8,9, Fig.1||||||21-JAN-16
25355|Nullarbor Limestone|31908|4|Described|Table 1|||L.Miocene||||||
25355|Nullarbor Limestone|31909|3|Fully described|p8|||Table 1. Fig.1||||||
25355|Nullarbor Limestone|31913|4|Described|Table 1|||See also Table 1||||||
25355|Nullarbor Limestone|31914|6|Mentioned|Pl.10|||||||||
25355|Nullarbor Limestone|31915|6|Mentioned|Map legend|middle Miocene|middle Miocene|||||||
25355|Nullarbor Limestone|31919|6|Mentioned|p39|||||||||
25355|Nullarbor Limestone|31923|6|Mentioned|p18|||||||||
25355|Nullarbor Limestone|31924|6|Mentioned|p2|||Refers Singleton (1954)||||||
25355|Nullarbor Limestone|32201|5|Briefly described|p6|||See also p7. Refraction survey.||||||21-JAN-16
25355|Nullarbor Limestone|32552|2|Defined|p87|early Miocene|early Miocene|See also p88.||||||21-JAN-16
25355|Nullarbor Limestone|32648|6|Mentioned|p32|||Miocene||||||
25355|Nullarbor Limestone|32750|4|Described|p306|||||||||
25355|Nullarbor Limestone|33586|4|Described|Table 1|||See also p15.||||||21-JAN-16
25355|Nullarbor Limestone|33589|4|Described|p11|||See also p12. M.Miocene.||||||21-JAN-16
25355|Nullarbor Limestone|34180|6|Mentioned|p229|||Miocene||||||
25355|Nullarbor Limestone|34192|6|Mentioned|Map legend|early Miocene|early Miocene|||||||
25355|Nullarbor Limestone|34194|6|Mentioned|Map legend|early Miocene|early Miocene|||||||
25355|Nullarbor Limestone|34232|6|Mentioned|p76|||Irregular cavities.||||||
25355|Nullarbor Limestone|34295|6|Mentioned|p38|||Fauna||||||
25355|Nullarbor Limestone|34308|5|Briefly described|p198|||Batesfordian - Balcombian. See Fig.84||||||
25355|Nullarbor Limestone|34615|6|Mentioned|p10|||||||||
25355|Nullarbor Limestone|34759|6|Mentioned|p60|||||||||
25355|Nullarbor Limestone|34958|6|Mentioned|p88|||||||||
25355|Nullarbor Limestone|35051|6|Mentioned|p204|||Analysis.||||||
25355|Nullarbor Limestone|35059|6|Mentioned|Table.19|||||||||
25355|Nullarbor Limestone|35097|6|Mentioned|p16|||||||||
25355|Nullarbor Limestone|35496|6|Mentioned|p23|||||||||
25355|Nullarbor Limestone|35772|4|Described|Table 1|||||||||
25355|Nullarbor Limestone|36200|6|Mentioned|p6|||||||||
25355|Nullarbor Limestone|36257|6|Mentioned|Table 2.1|||||||||
25355|Nullarbor Limestone|36890|3|Fully described|p415|||||||||
25355|Nullarbor Limestone|37132|5|Briefly described|p369|||||||||
25355|Nullarbor Limestone|37577|6|Mentioned|p75|||||||||
25355|Nullarbor Limestone|37852|6|Mentioned|Fig.3|||||||||
25355|Nullarbor Limestone|38016|6|Mentioned|p88|||||||||
25355|Nullarbor Limestone|38018|6|Mentioned|p124|||||||||
25355|Nullarbor Limestone|38068|6|Mentioned|Fig.7|||||||||
25355|Nullarbor Limestone|38553|6|Mentioned|p43|||||||||
25355|Nullarbor Limestone|38602|6|Mentioned|p2|||||||||
25355|Nullarbor Limestone|40003|5|Briefly described|Table 14|||See also Plate 18||||||
25355|Nullarbor Limestone|40298|6|Mentioned|Table II|||||||||
25355|Nullarbor Limestone|40410|6|Mentioned|p4|||||||||
25355|Nullarbor Limestone|40425|6|Mentioned|p46|||||||||
25355|Nullarbor Limestone|40466|6|Mentioned|p63|||||||||
25355|Nullarbor Limestone|40643|5|Briefly described|p148|||||||||
25355|Nullarbor Limestone|40992|6|Mentioned|Fig.23|||||||||
25355|Nullarbor Limestone|41043|6|Mentioned|p87|||||||||
25355|Nullarbor Limestone|41075|6|Mentioned|p18|||||||||
25355|Nullarbor Limestone|41505|6|Mentioned|p2|||||||||
25355|Nullarbor Limestone|41609|5|Briefly described|Fig.5|||||||||
25355|Nullarbor Limestone|42075|5|Briefly described|Fig.10 P250|||||||||
25355|Nullarbor Limestone|42265|5|Briefly described|p4|||||||||
25355|Nullarbor Limestone|42335|4|Described|p326|||||||||
25355|Nullarbor Limestone|42356|5|Briefly described|Fiche 7 P13|Miocene||||||||
25355|Nullarbor Limestone|42959|5|Briefly described|p58 Fig.3|||||||||
25355|Nullarbor Limestone|43026|5|Briefly described|Table 4,p590|||||||||
25355|Nullarbor Limestone|43040|6|Mentioned|p861|||||||||
25355|Nullarbor Limestone|43053|5|Briefly described|Map Legend|Miocene|Eocene|Geological Province: Eucla Basin.||||||25-MAY-05
25355|Nullarbor Limestone|43203|5|Briefly described|Map Legend||Miocene|Eucla Basin||||||
25355|Nullarbor Limestone|43258|5|Briefly described|Map Legend|Miocene|Eocene|||||||
25355|Nullarbor Limestone|43298|5|Briefly described|Map Legend|Miocene|Eocene|||||||
25355|Nullarbor Limestone|43498|5|Briefly described|8||Miocene|||||||
25355|Nullarbor Limestone|43713|5|Briefly described|p2||Miocene|||||||
25355|Nullarbor Limestone|43814|6|Mentioned|Fig.3,p115|||||||||
25355|Nullarbor Limestone|44133|5|Briefly described|p184, 180 Fig. 10.22|Middle Miocene|Middle Miocene|Geological Province: Eucla Basin. Overlies: Wilson Bluff Limestone. Thickness: 45m. Includes: Mullamullang Member.||||||
25355|Nullarbor Limestone|44145|4|Described|p550, p556-7, p555 fig 4-194, p548|Early Miocene|Early Miocene|Eucla Basin. Age from echinoid and foraminifera fauna. Max known thickness 31m. Type section at Wilson Bluff, east of Eucla.|||Mullamullang Limestone Member|Grades laterally northwards into Colville Sandstone and Plumridge Formation.|Bioclastic calcarenite, locally shelly.|08-OCT-15
25355|Nullarbor Limestone|44365|5|Briefly described|map legend|Pleistocene|Pliocene|||||||
25355|Nullarbor Limestone|44412|14|Not recorded|map legend||Early Miocene|L.Miocene.||||||
25355|Nullarbor Limestone|44695|5|Briefly described|Map Legend|Miocene|Miocene|(Early-Middle Miocene)||||||
25355|Nullarbor Limestone|44864|5|Briefly described|Map Legend||Miocene|||||||
25355|Nullarbor Limestone|45149|4|Described|p63|||||||||
25355|Nullarbor Limestone|46993|6|Mentioned|p262|||||||||
25355|Nullarbor Limestone|60953|5|Briefly described|Map Legend|Miocene|Eocene|Geological Province: Eucla Basin.||||||
25355|Nullarbor Limestone|61108|5|Briefly described|map legend|Miocene|Eocene|Geological Province: Eucla Basin.||||||
25355|Nullarbor Limestone|61155|5|Briefly described|p4, p17|Middle Miocene|Early Miocene|Partly overlies and interfingers with Colville Sandstone. Age: 18.5-14.5Ma. Max. thickness: 40m. Geological Province: Eucla Basin.||||||
25355|Nullarbor Limestone|61197|5|Briefly described|p473, p475, p478 Fig.4, p488-489|Middle Miocene|Early Miocene|Eucla Basin. Marine, shallow shelf deposits. 0-15m thick.|||||Well-cemented, foraminiferal and coralline algal calcarenite.|
25355|Nullarbor Limestone|61234|4|Described|p6, p7 Fig 4.|Early Pliocene|Middle Miocene|Unconformably overlies Wilson Bluff Limestone. Geological Province: Eucla Basin. Marine limestone.||||||14-MAY-07
25355|Nullarbor Limestone|61517|6|Mentioned|p312|||||||||27-MAY-06
25355|Nullarbor Limestone|61544|6|Mentioned|p367 Fig.3. |Eocene|Eocene|||||Overlies Pidinga Formation.||
25355|Nullarbor Limestone|62369|5|Briefly described|p409, p410 Fig.4|Middle Miocene|Early Miocene|Hard, fossiliferous, muddy limestone. Overlies the Abrakurrie Limestone. Geological Province: Eucla Basin.||||||
25355|Nullarbor Limestone|62640|5|Briefly described|pp70-77.     |Miocene|Miocene|Numerous large benthic fauna and relatively high proportion of aragonitic components indicate warmer-water conditions.|||Includes Mullamullang Member.|Overlies Abrakurrie Limestone.|Includes large benthic foraminifera and aragonitic material; well-cemented.|
25355|Nullarbor Limestone|65942|2|Defined|p77-78||Miocene|||Of Eucla Group.||||
25355|Nullarbor Limestone|66131|6|Mentioned|p242 Fig.2|Miocene|Miocene|Early to Middle Miocene in age (from p.242 Fig.2 - stratigraphic correlation chart).||||||
25355|Nullarbor Limestone|67117|5|Briefly described|Map legend.|Miocene|Eocene|Shown under general heading of 'Eocene - Miocene'. Covers over 99% of the map area.|||||Limestone, bioclastic, micritic; subtidal, platformal, above fair-weather wave-base.|03-MAY-13
25355|Nullarbor Limestone|67462|5|Briefly described|Map legend.|Miocene|Miocene|Bunda Plateau, Eucla Basin.||||||
25355|Nullarbor Limestone|67789|5|Briefly described|p33-36, 39, 41-46|Miocene|Miocene|Eucla Basin. Up to 45m thick. Forms the surface of the Nullarbor Plain. Contains shallow caves (tubes and vertical shafts/chambers) across the entire Plain. Comprises an estimated c.25% microkarst cavities (described).||Eucla Group.||Overlies Abrakurrie Limestone. Is overlain locally by Roe Calcarenite.|A hard, abundantly fossiliferous (listed) sub-tropical deposit. Laterally extensive grainstone to rudstone, extensively cemented by diagenetic low-Mg calcite spar. Lithologies described in detail.|
25355|Nullarbor Limestone|67921|5|Briefly described|Map legend|Pliocene|Miocene|Subcrop and minor outcrop.|||||Marine platform bioclastic limestone. Indurated and recrystallised with basal member of mud, sand and grit. Lagoonal, calcareous and dolomitic mudstone as at Ifould Lake. Lower part may be distinctly echinoidal. Upper part is foraminiferal.|
25355|Nullarbor Limestone|69004|5|Briefly described|p19, p34, p41, p115|Middle Miocene|Lower Miocene|Eucla Basin. Up to 25m thick in the Iluka Palaeovalley. Has restricted distribution in the Eucla Basin.||||Overlies the Pidinga Formation.|Carbonates including limestone.|
25355|Nullarbor Limestone|69297|5|Briefly described|p14 fig 2.4|Holocene|Lutetian|Eyre, Ceduna and Duntroon Sub-basins. See also p25 fig 2.9, p39 fig 2.14, p60.||||Overlies the Pidinga Formation.|Limestones.|
25355|Nullarbor Limestone|69386|6|Mentioned|p7|Miocene|Miocene|Eucla Basin.||||||
25355|Nullarbor Limestone|69598|5|Briefly described|p2, p9, p10, p11 Tb.1, p29 Tb.4|Pliocene|Middle Miocene|Eucla Basin. Up to 35m thick. Potential carbon dioxide storage reservoir.||||Overlies the Abrakurrie Limestone. Grades into and interfingers with the Colville Sandstone and Plumridge Formation.|Marine carbonates including limestone and foraminiferal algal calcarenites and rhodolith rudstones to floatstones.|
25355|Nullarbor Limestone|69632|5|Briefly described|p26-27, p30, p32|Miocene|Miocene|Eucla Basin. Early to middle Miocene. Most lithified unit in the Group, due to low-Mg calcite cement. Has extensive secondary porosity.||Eucla Group|||Limestone rich in coralline algae (rhodoliths and articulated types), large and small benthic foraminifera, and molluscs.|09-OCT-18
25355|Nullarbor Limestone|69648|4|Described|p4,p6 Fig.3,p20 Plate3,p23,p25-27,p32-33|Miocene|Miocene|Basement highs with thin cover. Semi-arid - arid karst region: immature karst. Nullabor Plain, Eucla Basin. Age: deposited early Middle Miocene. Marine platform bioclastic carbonates; locally at base is thin (20-30 cm) transgressive lag (v.poorly sorted, non-calcareous, clay, sand, grit); basal 1-2 m limestone (trace quartz grains); most of overlying limestone has no terrigenous clastic component; mostly foraminifera-rich packstone. Best exposed on cliffs of Great Australian Bight and in quarries (~12 m at Watson). Overall uniformity of thickness (20-35 m) across platform, that extends beneath dunefield. See also map legend.|~15 Ma|Eucla Group||Overlies palaeochannels of Pidinga Formation; no evidence of intertonguing with Hampton Sandstone; sharply overlies Yarle Sandstone.|Locally thin base of terrigenous lag (20-30 cm), basal (1-2 m) limestone (trace quartz), no terrigenous component to most of overlying limestone; predominantly indurated, recrystallised, micritic, bioclastic, white, off-white to grey limestone.|
25355|Nullarbor Limestone|70067|6|Mentioned|Ceduna: Fig.2. Regional: Fig.2|Holocene|Eocene|Bight Basin.||||||
25355|Nullarbor Limestone|70337|5|Briefly described|Map legend.|Miocene|Eocene||||||Limestone, bioclastic, micritic. Subtidal, platformal, above fair-weather wave-base.|
25355|Nullarbor Limestone|70397|4|Described|p1-8,10-13|Middle Miocene|Middle Miocene|Eucla Basin. Extremely fossiliferous; contains large benthic foraminifera and zooxanthellate corals. Comprises five main facies and subfacies. See p3-11 for detailed lithofacies descriptions. See also Table 1 p6 for summary. Deposition coincides with the Miocene Climatic Optimum, a time of elevated temperatures worldwide that caused expansion of tropical waters and associated organisms into higher latitudes (McGowran et al., 1997b).||Unit of Eucla Group.|Includes Rawlinna member and Mullamullang Member.|Onlaps on Abrakurrie Limestone and Wilson Bluff limestone (inboard). Laterally grades inboard (N-ward) into Colville Sandstone. Overlies the Eucla Group. Unconformably overlain by the Roe Calcarenite.|Rhodolith Facies, Articulated Coralline Algae Facies, Benthic Foraminifera Facies, Echinoid Facies, and Planktonic Foraminifera Facies.|29-JUL-19
25355|Nullarbor Limestone|70771|4|Described|p3-p4, p7, p11-p13, p15, p21, p27|Middle Miocene|Early Miocene|Eucla Platform, Eucla Basin.  [The author assigns this unit to the Eucla Group however this term is obsolete]. See also p31, p33, p39-p40, p53-p58, p60-p61.||Eucla Group|Includes the Mullamullang Member.|Disconformably overlies the Abrakurrie Limestone.||
25355|Nullarbor Limestone|70778|5|Briefly described|p4, p10|||Intersected in Nundroo 3 DDH.|||||Limestone, calcareous mudstone.|
25355|Nullarbor Limestone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||limestone, calcarenite|
25355|Nullarbor Limestone|71361|4|Described|ii, p1-p3, p5-p6, p15, p17-p20, |Middle Miocene|Early Miocene|Eucla Basin. [NB that the Eucla Group to which the author assigns this unit is currently in disuse]. This unit has a rich fossil assemblage containing coralline algae, large and small benthic foraminifera and molluscs; diverse zooxanthellate corals are also present but not numerous. Fossil assemblage, palaeoenvironments and facies are discussed in great detail. This unit is interpreted to have been deposited in three main palaeoenvironments: rhodolith gravels, seagrass banks and open seafloors. See also p22-p23, p25-p28, p31, p33-p34, p37, p39, p41-p51, p53-p81, p117, p119-p120, p122-p123, p129, p135, p137-p145, p148-p160.||Eucla Group|Includes the Mullamullang Limestone Member.|Unconformably overlies the Wilson Bluff Limestone and the Abrakurrie Limestone. Unconformably overlain by the Roe Calcarenite. Equivalent to (grades into) the Colville Sandstone.|Fine to coarse grained fossiliferous calcarenites.|
25355|Nullarbor Limestone|71618|6|Mentioned|p124|Cenozoic|Cenozoic|Geological province: Eucla Basin.||Unit of Eucla Group.||||
25355|Nullarbor Limestone|71758|14|Not recorded|p81|||In 1967 Annual Report.||||||
25355|Nullarbor Limestone|71891|5|Briefly described|p6-p7, p14, p29-p52, p54-p55|Cenozoic|Cenozoic|Eucla Basin, Coompana Province. 20-35m thick unit interpreted to have been deposited in a shallow platform setting with a paucity or terrigenous material suggesting river systems carried little debris to the coast.||||Overlies the Abrakurrie Limestone.|Hard, chalky limestone.|
25355|Nullarbor Limestone|72344|5|Briefly described|p5, p16, p49, p61|||Eucla Basin. 20-35m thick. Includes large benthic foraminifera and aragonitic material. Interpreted to have been deposited in a shallow platform setting with the paucity of terrigenous material suggesting river systems carried little debris to the coast. See also p84, p96, p160, p169.||||Overlies the Abrakurrie Limestone.|Limestone, bioclastic, micritic subtidal, platformal, above fair weather wave-base.|
25355|Nullarbor Limestone|72465|5|Briefly described|p9, 15, 17|Tertiary|Tertiary|Eucla Basin, Coompana Province. 20-35m thick. Forms the ""lumpy"" brown, parallel-bedded unit at the top of the Bunda Cliffs.||||Overlies Abrakurrie Limestone.|Limestone, bioclastic, micritic. Subtidal, platformal, above fair-weather wave-base. Includes large benthic foraminifera and aragonitic material, well-cemented.|
25355|Nullarbor Limestone|72466|5|Briefly described|p9, 15, 17|Tertiary|Tertiary|Benbow et al. (1995). Eucla Basin, Coompana Province. 20-35m thick. Deposited in a shallow platform setting. Forms the ""lumpy"" brown, parallel-bedded unit at the top of the Bunda Cliffs.||||Overlies Abrakurrie Limestone.|Limestone, bioclastic, micritic, subtidal, platformal, above fair-weather wave-base. Includes benthic foraminifera and aragonitic material; well-cemented.|
25355|Nullarbor Limestone|72467|5|Briefly described|p9, p15, 17|Tertiary|Tertiary|Eucla Basin, Coompana Province. 20-35m thick. Forms the ""lumpy"" brown, parallel-bedded unit at the top of the Bunda Cliffs.||||Overlies Abrakurrie Limestone.|Limestone, bioclastic, micritic. Subtidal, platformal, above fair-weather wave-base. Includes large benthic foraminifera and aragonitic material, well-cemented.|
25355|Nullarbor Limestone|72468|5|Briefly described|p9, p15, p17|||Eucla Basin. 20-35 m thick. Deposited in a shallow platform setting, with the paucity of terrigenous material suggesting river systems carried little debris to the coast. Forms the 'lumpy' brown, parallel-bedded unit at the top of the Bunda Cliffs.||||Underlain by Abrakurrie Limestone.|Limestone, bioclastic, micritic. Subtidal, platformal, above fair weather wave-base. Includes large benthic foraminifera and aragonitic material; well-cemented.|
25355|Nullarbor Limestone|72469|5|Briefly described|p9, p15, p17|||Eucla Basin. 20-35 m thick. Deposited in a shallow platform setting, with the paucity of terrigenous material suggesting river systems carried little debris to the coast. Forms the 'lumpy' brown, parallel-bedded unit at the top of the Bunda Cliffs.||||Underlain by Abrakurrie Limestone.|Limestone, bioclastic, micritic. Subtidal, platformal, above fair weather wave-base. Includes large benthic foraminifera and aragonitic material; well-cemented.|
25355|Nullarbor Limestone|72470|5|Briefly described|p9, p15, p18|||Eucla Basin. 20-35 m thick. Deposited in a shallow platform setting, with the paucity of terrigenous material suggesting river systems carried little debris to the coast. Forms the 'lumpy' brown, parallel-bedded unit at the top of the Bunda Cliffs.||||Underlain by Abrakurrie Limestone.|Limestone, bioclastic, micritic. Subtidal, platformal, above fair weather wave-base. Includes large benthic foraminifera and aragonitic material; well-cemented.|
25355|Nullarbor Limestone|72471|5|Briefly described|p9, p15, p17|||Eucla Basin. 20-35 m thick. Deposited in a shallow platform setting, with the paucity of terrigenous material suggesting river systems carried little debris to the coast. Forms the 'lumpy' brown, parallel-bedded unit at the top of the Bunda Cliffs.||||Underlain by Abrakurrie Limestone.|Limestone, bioclastic, micritic. Subtidal, platformal, above fair weather wave-base. Includes large benthic foraminifera and aragonitic material; well-cemented.|
25355|Nullarbor Limestone|72472|5|Briefly described|p9, p15-16|||Eucla Basin. 20-35 m thick. Deposited in a shallow platform setting, with the paucity of terrigenous material suggesting river systems carried little debris to the coast. Forms the 'lumpy' brown, parallel-bedded unit at the top of the Bunda Cliffs.||||Underlain by Abrakurrie Limestone.|Limestone, bioclastic, micritic. Subtidal, platformal, above fair weather wave-base. Includes large benthic foraminifera and aragonitic material; well-cemented.|
25355|Nullarbor Limestone|73084|5|Briefly described|p16-17|Eocene|Eocene|Eucla Basin||||Underlain by Wilson Bluff Limestone.|Hard, chalky limestone.|
25355|Nullarbor Limestone|73101|5|Briefly described|Map legend.|Miocene|Eocene||||||Limestone, bioclastic, micritic. Subtidal, platformal, above fair-weather wave-base.|
25355|Nullarbor Limestone|73108|5|Briefly described|Map legend.|Miocene|Eocene||||||Limestone, bioclastic, micritic. Subtidal, platformal, above fair-weather wave-base.|
25355|Nullarbor Limestone|73112|5|Briefly described|Map legend.|Miocene|Miocene|||||Locally overlies Abraukurrie Limestone.|Yellow-brown, hard, recrystallised fossiliferous limestone|
25355|Nullarbor Limestone|73641|5|Briefly described|p5-11, 13-15|Miocene|Miocene|Eucla Basin. 20-35m thick. Subtidal, above wave-base, deposits. Features numerous large caves, karst pocket valleys, and thousands of sub-metre scale blowholes. Local calcrete induration to the SE. Is blanketed by 10-20 cm thick layer of calcareous soil. Photographs. Mineralogical, elemental, TOC compositions tabulated.||||Overlies Abrakurrie Limestone.|Bioclastic micritic limestone.|
35082|Nultaddy seismic unit|23054|5|Briefly described|p17-8||Devonian|||||||
83062|Nummee Granodiorite|73104|4|Described|p: 1, 3, 5, 24-26, 29, 32-33, 36-37, 51|Statherian|Statherian|Identified as a distinct stratigraphic unit during the Southern Gawler Ranges Margin mapping program and formally defined within the Mount Double Explanatory Notes. Exposed in the Waulkinna Hill area. Represents the easternmost recognised unit within the Tunkillia Suite. Geochon represents magmatic crystallisation age, which places it within the age range of the Tunkillia Suite. This interpretation is consistent with geochemical signatures. Microgranite dykes interpreted as late stage phases of the granodiorite intrusion. Sample also contained an inherited zircon population at 1723 +/- 6 Ma interpreted as assimilation of zircon from xenoliths [possibly of Peter Pan Suite]. Contains a laterally continuous zone approximately 50 m wide and 3 m thick which contains xenoliths of a fine- to medium-grained, compositionally layered quartz-feldspar-biotite metamorphic rock. [Article includes petrographic description].|1692 +/- 4 Ma|Tunkillia Suite||Intruded by Gawler Range Volcanics dykes.|Feldspar-megacrystic to equigranular granitoid containing microgranite dykes.|
24435|Nuyts Volcanics|22613|6|Mentioned|p14|||||||||
24435|Nuyts Volcanics|22629|6|Mentioned|fig2p147|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
24435|Nuyts Volcanics|24197|6|Mentioned|p74 Tb. 8.1|Paleoproterozoic|Paleoproterozoic|Age: 1625Ma. Geological Province:||||||07-FEB-11
24435|Nuyts Volcanics|42291|6|Mentioned|Fig.1 P3|||Variation of Nuyts Archipelago volcanics?||||||
24435|Nuyts Volcanics|42404|6|Mentioned|p32|||||||||
24435|Nuyts Volcanics|42466|5|Briefly described|Map Legend|||||||||
24435|Nuyts Volcanics|42469|6|Mentioned|p22|||Great Australian Bight region||||||
24435|Nuyts Volcanics|42470|6|Mentioned|p17|||||||||
24435|Nuyts Volcanics|42475|4|Described|p14|||||||||
24435|Nuyts Volcanics|43052|5|Briefly described|p69|||||||||
24435|Nuyts Volcanics|43053|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Rhyolite, rhyodacite.||||||07-NOV-08
24435|Nuyts Volcanics|43086|5|Briefly described|Appendix, Stop 7|||Age of 1630 Ma.||||||12-JUL-16
24435|Nuyts Volcanics|43258|5|Briefly described|Map Legend||Mesoproterozoic|||||||
24435|Nuyts Volcanics|43298|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
24435|Nuyts Volcanics|50605|5|Briefly described|p(i), 1.3, 7.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Gawler Craton & Curnamona Province. Of the Saint Peter Suite. Age: 1631-1627 +/- 3Ma (U-Pb).||||||07-NOV-08
24435|Nuyts Volcanics|60953|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Age: 1631-1627Ma. Rhyodacite to rhyolite.||||||07-NOV-08
24435|Nuyts Volcanics|61108|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|Rhyodacite to rhyolite. Age: 1631-1627 Ma.||||||07-NOV-08
24435|Nuyts Volcanics|63020|5|Briefly described|p986, p987 Fig. 8|Paleoproterozoic|Paleoproterozoic|Age: 1631+/-3Ma. Geological Province: Gawler Craton (Nuyts Domain).||||||07-NOV-08
24435|Nuyts Volcanics|63866|5|Briefly described|p6, p9, p31|Statherian|Statherian|Nuyts Domain, Gawler Craton.|c. 1630 Ma (Rankin et al., 1990)|||||
24435|Nuyts Volcanics|64130|5|Briefly described|p1378 Fig.1, p1380 Fig.2, p1382  |Mesoproterozoic|Mesoproterozoic|SW Gawler Craton.|ca. 1630 Ma|||Intruded by the St. Peter Suite.|Alkaline, porphyritic rhyodacite to rhyolite.|
24435|Nuyts Volcanics|64576|6|Mentioned|p625 Fig. 2|Mesoproterozoic|Mesoproterozoic|Age: 1640-1620Ma. ||||||
24435|Nuyts Volcanics|65376|5|Briefly described|p10. |||Slightly older than the 'associated' St Peter Suite.|1631 +/- 3 Ma to 1627 +/- 2 Ma.|||||
24435|Nuyts Volcanics|65390|6|Mentioned|p22 Fig. 3|Statherian|Statherian|Age of 1630 Ma given.||||||
24435|Nuyts Volcanics|65772|6|Mentioned|p229 Fig.2|Statherian|Statherian|1640-1620 Ma||||||
24435|Nuyts Volcanics|65922|5|Briefly described|p29 Fig. 6, p31|Statherian|Statherian|Felsic. Intruded by or comagmatic with St Peter Suite. Age of ~1630 Ma given.||||||
24435|Nuyts Volcanics|66302|5|Briefly described|p24, p33, p34, p76 Fig.20|Statherian|Statherian|Nuyts Domain, Gawler Craton. Another age given at 1627 +/- 2 Ma (TIMS zircon, Flint and Rankin, 1991)|1631 +/- 3 Ma (TIMS zircon, Cooper et al, 1985)||||Dark grey to pink porphyritic rhyodacite to rhyolite.|
24435|Nuyts Volcanics|67058|6|Mentioned|p477 Fig. 1|Paleoproterozoic|Paleoproterozoic|Listed with St Peter Suite.|1640-1620 Ma.|||||19-APR-12
24435|Nuyts Volcanics|67181|5|Briefly described|p616 Fig.1|Paleoproterozoic|Paleoproterozoic|Gawler Craton. References: Fairclough et al. 2003, Payne et al. 2003.|1640-1620 Ma|||||
24435|Nuyts Volcanics|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Southern Gawler Craton.|1631 +/- 3 Ma to 1627 +/- 2 Ma.|||||
24435|Nuyts Volcanics|67536|5|Briefly described|Map Legend|Statherian|Statherian|Gawler Craton.|1631 +/- 3 Ma - 1627 +/- 2 Ma||||Rhyodacite to rhyolite.|
24435|Nuyts Volcanics|67900|5|Briefly described|p20|Paleoproterozoic|Paleoproterozoic|Rankin et al. (1990). SW Gawler Craton.|c.1630 Ma (Rankin et al., 1990).||||Significant volume of moderately juvenile bimodal magmatism.|
24435|Nuyts Volcanics|69048|6|Mentioned|p3|||Central-western Eyre Peninsula.||||||
24435|Nuyts Volcanics|69255|5|Briefly described|p788|Statherian|Statherian|Rankin et al. (1990). Gawler Craton.|c.1630 Ma.||||Bimodal volcanics.|
24435|Nuyts Volcanics|70286|6|Mentioned|p884|Paleoproterozoic|Paleoproterozoic|Eastern Gawler Craton.|1630-1608 Ma.|||||
24435|Nuyts Volcanics|70893|6|Mentioned|p3 fig 1b|Paleoproterozoic|Paleoproterozoic|||||||
24435|Nuyts Volcanics|71129|6|Mentioned|p18|Statherian|Statherian|Geological Province: Nuyts Domain, Gawler Craton.|1630 Ma|||||
24435|Nuyts Volcanics|71317|5|Briefly described|p16|Palaeoproterozoic|Palaeoproterozoic|Nuyts Domain, Gawler Craton.|c. 1630 Ma|||||
24435|Nuyts Volcanics|71348|6|Mentioned|p201|Statherian|Statherian|Geological province: Gawler Craton.||||||
24435|Nuyts Volcanics|71712|6|Mentioned|p411, 419|Statherian|Statherian|Eastern Gawler Craton. Located west of the Cariewerloo Basin.|~1630 Ma|||||
24435|Nuyts Volcanics|71859|6|Mentioned|p4-p5|Statherian|Statherian|Nuyts Domain, southern Gawler Craton.|c. 1630 Ma (Rankin et al., 1990)|||||
24435|Nuyts Volcanics|71862|5|Briefly described|p4|Paleoproterozoic|Paleoproterozoic|Southwestern Gawler Craton.|c. 1630 Ma||||Felsic volcanics.|
24435|Nuyts Volcanics|72090|6|Mentioned|p10, p11|Statherian|Statherian|Nuyts Domain, Gawler Craton.|c. 1630 Ma|||||
24435|Nuyts Volcanics|73026|5|Briefly described|p6, p10,|Mesoproterozoic|Paleoproterozoic|Southwestern Gawler Craton.|c. 1625 Ma|||Intruded by the St Peter Suite.|Rhyodacitic to rhyolitic volcanics.|
24435|Nuyts Volcanics|73027|5|Briefly described|p6, p9|||Southwestern Gawler Craton.|c. 1630 Ma|||||
24435|Nuyts Volcanics|73235|6|Mentioned|p53, p63|Statherian|Statherian|Gawler Craton. Nuyts region. Hosts gold mineralisation in the Western Gawler mineral field of the Kararan (Hiltaba Suite) gold mineral system.|1630 Ma|||||
24435|Nuyts Volcanics|73302|5|Briefly described|p32, p34-35, p53|Palaeoproterozoic|Palaeoproterozoic|Gawler Craton. Geochronology by Cooper et al. (1995) and Rankin et al. (1990) respectively. Mis-spelt as Nyuts (Volcanics) on p32.|1631 +/- 3 Ma; 1627 +/- 2 Ma.|||Is intruded by Saint Francis Granite. Coeval with St Peter Suite and Saint Francis Suite.|Volcanics and porphyritic intrusives: porphyritic rhyodacite and rhyolite; intruded by rhyodacite to rhyolite dykes and a distinctive leucogranite (the Saint Francis Granite).|02-MAR-23
74092|Old Boolcoomata Conglomerate Member|62724|2|Defined|p19-22|Cryogenian|Cryogenian|Of Benda Siltstone (Yudnamutana Subgp, Umberatana Gp). Overlain by + interfingers with Benda Siltstone. Max. thick: 450m. Geol.Prov: MacDonald Corridor. See also p17 Fig. 4, p18. Age shown as Sturtian p17, but said to be Neoproterozoic, Cryogenian i.e. 800-~600 Ma, p20.||||||29-AUG-18
74092|Old Boolcoomata Conglomerate Member|62993|4|Described|p5, p3, p44.|Neoproterozoic|Neoproterozoic|Sturtian metasediments.||Benda Siltstone|||Oligomictic conglomerate with two mica s-type granite clasts. Also with clasts of psammitic and albitic metasediments, migmatite and mica schist. Clasts vary from sub angular to well rounded.|19-DEC-21
74092|Old Boolcoomata Conglomerate Member|70405|4|Described|p51 Table 4, p57|Neoproterozoic|Neoproterozoic|||Yudnamutana Subgroup|||Proximal, clast supported, pebble-boulder sized granite clastic, massive glacial conglomerate interfingered with gritty arkosic facies that is commonly cross bedded.|
29892|Old Camp Granite|22631|6|Mentioned|p176|Calymmian|Calymmian|||||||
29892|Old Camp Granite|24197|5|Briefly described|p75 Tb. 8.1|Mesoproterozoic|Mesoproterozoic|Age: 1560Ma.||||||07-FEB-11
29892|Old Camp Granite|43052|5|Briefly described|Table 4.8|||||||||
29892|Old Camp Granite|50605|5|Briefly described|p(iii), 1.4, 10.2, Table 1.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Gawler Craton & Curnamona Province. Of the Moolawatana Suite. Age: ~1560Ma.||||||
29892|Old Camp Granite|62962|5|Briefly described|p2284 Fig. 2|Mesoproterozoic|Mesoproterozoic|Age: 1555+/-8Ma (Fanning, 1995). Geological Province: Mount Painter Province.||||||07-FEB-11
29892|Old Camp Granite|66302|6|Mentioned|p50|Calymmian|Calymmian|Moolawatana Domain, Curnamona Province.|1555 +/- 8 Ma (Fanning et al, 1998)|Moolawatana Suite||||
29892|Old Camp Granite|70384|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic||1554 +/- 12 Ma (SHRIMP U-Pb zircon).||||Granite, red, massive, structureless and strongly lineated, variable grainsize. Plagioclase, K-feldspar, quartz, magnetite and biotite.|
29892|Old Camp Granite|72459|6|Mentioned|p67|||Represents, alongside other small granite bodies like the Camel Pad Granite, the only known outcrop of 1555-1560 Ma Moolawatana magmatism in the SE Mt Painter Inlier.|1555-1560 Ma|Moolawatana Suite||||
75789|Old Mount North West Member|66884|2|Defined|p37-44, incl Figs.2-4|||New name. Type section: outcrops along Willouran Creek (29deg52.420'S, 138deg0.560'E to 29deg52.000'S, 138deg1.620'E). Thickness: ~1040 m thick in type section, but thins to ~500 m adjacent to Witchelina diapir. Age: Mid Torrensian. Old Mount North West Member and lower member of Myrtle Springs Formation encompass strata previously defined as uppermost Burra unit (Coats 1973), Burra Group (Forbes and Coats 1963; Forbes et al. 1965; Forbes 1990) and Myrtle Springs Formation (Preiss 1986; Belperio 1987, 1990; Forbes 1988; Dyson 2000). Previously mapped as lower portion of Myrtle Springs Formation.||Skillogalee Dolomite||Overlies Twenty Mile Hill Member; is disconformably overlain by lower member of Myrtle Springs Formation; juxtaposed against Umberatana Group and diapiric breccia west of Trial Hole.|Calcareous quartz arenite (thin-medium bedded to thinly laminated, well indurated to flaggy, fine- to medium-grained), interbedded with sandy dolostone and dolostone with chert nodules; red-brown weathered and blue-grey fresh.|14-DEC-16
29898|Olympic Dam Breccia Complex|22629|6|Mentioned|p159|||Hosted by the Roxby Downs Granite||||||
29898|Olympic Dam Breccia Complex|22645|6|Mentioned|P204|||||||||
29898|Olympic Dam Breccia Complex|23805|4|Described|p5|Mesoproterozoic|Mesoproterozoic|Hosted by Rxby Downs Granite.  Consists of funnel-shaped, barren, haematite-quartz breccia 'core' surrounded by an irregular array of variably mineralised and broadly zoned haematite-granite breccia.  Geological Province: Gawler Craton.||||||
29898|Olympic Dam Breccia Complex|24261|3|Fully described|p1046|Calymmian|Calymmian|Geological Province: Gawler Craton. Age: ~1590Ma. Parent: Roxby Downs Granite||||||
29898|Olympic Dam Breccia Complex|43052|4|Described|p132|||||||||
29898|Olympic Dam Breccia Complex|50081|6|Mentioned|p42|||Geological Province: Gawler Craton.||||||24-FEB-05
29898|Olympic Dam Breccia Complex|50605|5|Briefly described|p8.8|||||||||
29898|Olympic Dam Breccia Complex|60515|5|Briefly described|p120, p122, p124 Fig.8|||Hosts the world-class Olympic Dam Cu-Au-Ag-U deposit (described in some detail).||||Hosted by the Roxby Downs Granite.||
29898|Olympic Dam Breccia Complex|61522|5|Briefly described|p4|||A zoned breccia derived from, and hosted by, Roxby Downs Granite. The Olympic Dam orebody is wholly contained within this breccia complex.||||||
29898|Olympic Dam Breccia Complex|64131|6|Mentioned|p1400|||Reeve et al. (1990). Brecciation was initiated by intrusion of mafic-felsic plutons below. Immediate wall rocks are unlikely to have been the source for ore metals.||||||
29898|Olympic Dam Breccia Complex|64132|6|Mentioned|p1431.|||Magnetite and hematite at Olympic Dam are argued (Haynes et al. 1995) to have formed essentially coevally in different parts of this Complex, during multiple overprinting hydrothermal cycles.||||||
29898|Olympic Dam Breccia Complex|64133|5|Briefly described|p1447 Tb.1, p1464-1465|||Hosts the giant Olympic Dam deposit. Was an active intrusive and probably extrusive centre during breccia formation and alteration.||Unit in Roxby Downs Granite.|||Multistage hematitic breccias; volcaniclastics, felsic and mafic-ultramafic dykes.|
29898|Olympic Dam Breccia Complex|64559|6|Mentioned|p976, p977 Fig.11|||Hosted within Roxby Downs Granite.||||||23-DEC-08
29898|Olympic Dam Breccia Complex|64725|5|Briefly described|p69.|Mesoproterozoic|Mesoproterozoic|Forms a basement high under 300m of Neoproterozoic and Cambrian sedimentary rocks. Hosts the Olympic Dam deposit: a number of large dyke-like breccia bodies with Cu, Au, Ag, U and REE mineralisation.||Unit in Roxby Downs Granite.|||Bodies of brecciated granite surrounding heterolithic breccia, consisting of fragments of hematite, crushed and altered granite, grading into hematite-quartz microbreccia in central parts.|
29898|Olympic Dam Breccia Complex|64741|5|Briefly described|p311 Fig. 17|||Geological province: Gawler Craton.||||||07-FEB-11
29898|Olympic Dam Breccia Complex|65390|5|Briefly described|p10, p25|Calymmian|Calymmian|Contained within Roxby Downs Granite. Hosts Olympic Dam Cu-U-Au-Ag-REE deposit. Age of c. 1590 Ma given.||||||
29898|Olympic Dam Breccia Complex|70328|6|Mentioned|p160,163|||Contact with Olympic Dam dolerite is characterised by chilled margins.||||Intruded by Olympic Dam dolerite.||
29898|Olympic Dam Breccia Complex|70502|5|Briefly described|p17-18, 21-22, 26-27, 29|||Gawler Craton. Hosts the supergiant Olympic Dam Cu-U-Au-Ag (IOCG) deposit. Major and trace element composition of 26 samples are tabulated. U and Sm isotope compositions tabulated, discussed.||Roxby Downs Granite.||Is intruded by Gawler Range Volcanics dykes.|Weakly to intensely hematite +/- sericite-altered clasts of host granite, bedded clastic facies (i.e. interbedded mudstones, sandstones, conglomerates), and feldspar-phyric Gawler Range Volcanics in a fine-grained hematite-rich matrix.|
29898|Olympic Dam Breccia Complex|70511|5|Briefly described|p85-86, 88-89, 91, 96-99|Mesoproterozoic|Mesoproterozoic|Gawler Craton. Hosts the Olympic Dam Cu-U-Au-Ag (IOCG) deposit. Abbreviated to ODBC in most of the article. The five facies associations of the bedded clastic facies are described in detail; numerous photographs, photomicrographs.||||Is intruded by Gairdner Dyke Swarm and Gawler Range Volcanics.|Weakly to intensely hematite-altered granite clasts in a fine-grained hematite-rich matrix containing fine-grained disseminated ore minerals; large domains of polymictic breccia (of Gawler Range Volcanics) and two areas of bedded clastic facies.|
29898|Olympic Dam Breccia Complex|70659|5|Briefly described|p47-48|||Synchronous with Gawler Range Volcanic event. Described as tectonic-hydrothermal. Hosts IOCG-U mineralisation.|||||Laminated mudstone, thinly to medium bedded, graded to massive sandstone and thick conglomerate beds.|
29898|Olympic Dam Breccia Complex|70738|6|Mentioned|p189|||NE Gawler Craton. Hosts the Olympic Dam Cu-U-Au-Ag deposit.||||Entirely within Roxby Downs Granite.||
29898|Olympic Dam Breccia Complex|70947|4|Described|p961, 962, 968, 971|||[Is this a stratigraphic unit, or some kind of structural/mineralising feature?] Areal extent approximately 50 km2 at contact with overlying Stuart Shelf sedimentary rocks. Mineralogy discussed.||Of Roxby Downs Granite||Intruded by Gairdner Dyke Swarm. Gradational contact with Roxby Downs Granite.|Weakly to intensely altered and brecciated clasts of the major and minor constituent rock types - granite, altered felsic feldspar phyric lavas (from Gawler Range Volcanics), bedded clastic facies and mafic-ultramafic lavas/dykes.|
29898|Olympic Dam Breccia Complex|72488|6|Mentioned|p4|||||||||
29898|Olympic Dam Breccia Complex|72949|6|Mentioned|p36|Calymmian|Calymmian|Olympic Domain, north. Olympic Dam / Punt Hill area. Related to[?] Roxby Downs Granite.|1594 +/- 0.2 Ma|||||
29898|Olympic Dam Breccia Complex|73162|6|Mentioned|p459, p460|||Interpreted to represent relicts of a syn-Gawler Range Volcanics sedimentary basin. Detrital zircon age from bedded clastic facies is ca. 1590 Ma.|ca. 1590 Ma||||Includes mudstone, sandstone, and polymictic volcanic conglomerate. Intruded by high Mg, olivine-phyric basalt, dolerite and porphyritic mafic dykes.|
29898|Olympic Dam Breccia Complex|74361|5|Briefly described|p162, 164, 166, 171, 173-177|||Gawler Craton. Comprises numerous, irregularly shaped breccia bodies, formed along faults after emplacement of Gawler Range Volcanics and Roxby Downs Granite. Hosts the world-class Olympic Dam Cu-U-Au-Ag deposit. After the first page, it is referred to as ODBC throughout the article. Was initially overlain unconformably by Pandurra Formation (which was subsequently eroded).|||Includes clasts of Gawler Range Volcanics.|Occurs within the Roxby Downs Granite. Is intruded by Gairdner Dolerite dykes. Is overlain unconformably by Nuccaleena Dolomite.|Mainly comprises clasts of variably hematite-altered granite; clasts of mafic-ultramafic, felsic volcanic, and various bedded clastic facies, are locally dominant.|
39898|Oodla Wirra Volcanics|61238|2|Defined|p51|Neoproterozoic|Neoproterozoic|Of the Callanna Group. Age: 799+/-4 Ma to 798+/-5 Ma. Felsic volcanics, including pyroclastic and volcanic deposits. Inferred minimum thickness: 200m. See also p44-45, p46 Fig. 2, p47 Fig. 3||||||14-MAY-07
39898|Oodla Wirra Volcanics|64647|5|Briefly described|p44, p46|Willouran|Willouran|Age: 798+/-5 and 799+/-4Ma (Fabris et al. 2005). Felsic volcanism.||||||
39898|Oodla Wirra Volcanics|67536|5|Briefly described|Map Legend|Cryogenian|Cryogenian||ca. 802 +/- 10 Ma||||Felsic volcanic rocks.|
39898|Oodla Wirra Volcanics|72238|5|Briefly described|p42|Tonian|Tonian|Of Adelaide Geosycline. Age of 798+\-5 and 799+\-4 Ma (Fabris et al., 2005).||||||
39898|Oodla Wirra Volcanics|73262|6|Mentioned|p581|Tonian|Tonian|Marks the second phase of [Rodinian] rifting alongside the Rook Tuff of the proximal Callanna Group.|ca 798 Ma|||||
39898|Oodla Wirra Volcanics|74367|5|Briefly described|p8, p12, p18|Tonian|Tonian|Within the Nackara Arc. Coeval with Rook Tuff.|798+/-5 Ma, 799+/-4 Ma SHRIMP igneous zircon|Curdimurka Subgroup||||
24441|Oolarinna Member|22922|5|Briefly described|33 fig 2|Early Cambrian|Early Cambrian|Of Observatory Hill Formation, Officer basin. Oil show.||||||
24441|Oolarinna Member|23282|2|Defined|p76||Early Cambrian|Age: Early Cambrian 521 - 520Ma. of Observatory Hill Formation, Officer Basin. of Benbow (1982).||||||
24441|Oolarinna Member|24112|5|Briefly described|p254 Fig.2|Early Cambrian|Early Cambrian|Of the Marla Group. Geological Province: Officer Basin||||||
24441|Oolarinna Member|38329|2|Defined|p199|Early Cambrian|Early Cambrian|||||||
24441|Oolarinna Member|40945|6|Mentioned|p3|||||||||
24441|Oolarinna Member|42816|6|Mentioned|p14|||of Observatory Hill Formation||||||
24441|Oolarinna Member|43743|6|Mentioned|Fig.2,p33||Early Cambrian|||||||
24441|Oolarinna Member|44133|5|Briefly described|p37|Middle Paleozoic|Early Paleozoic|Of the Observatory Hill Formation. Thickness: 45m. Overlies: Relief Sandstone, Rodda beds (disc).||||||07-NOV-08
24441|Oolarinna Member|62570|5|Briefly described|p580 Figs. 2 and 3|Middle Cambrian|Middle Cambrian|Of Observatory Hill Formation (Marla Group). Geological Province: Officer Basin.||||||10-AUG-07
24441|Oolarinna Member|65313|5|Briefly described|p578 Fig. 6|Cambrian|Cambrian|Officer Basin.||Of Observatory Hill Formation.||Underlies Arcoeillinna Member, overlies Moyles Creek Chert Member.||26-MAR-12
24441|Oolarinna Member|72478|6|Mentioned|p8, digital p69|Early Cambrian|Early Cambrian|Officer Basin. See also Fig 7 p70.||Observatory Hill Formation||||29-MAR-21
24441|Oolarinna Member|73099|5|Briefly described|Map legend.|Middle Cambrian|Early Cambrian|Officer Basin.||Observatory Hill Formation.||Overlies Moyles Chert Marker Bed. Is overlain by Arcoeillinna Sandstone.|Reddish, micaceous siltstone, partly calcareous and dolomitic, and minor micaceous, very fine- to fine-grained sandstone.|
27068|Oolgelima Gravel|38604|6|Mentioned|Map legend|Quaternary|Quaternary|||||||
27068|Oolgelima Gravel|38605|4|Described|p40|||||||||
27068|Oolgelima Gravel|44133|5|Briefly described|p243|Quaternary|Quaternary|||||||
78310|Ooloo Hill Formation|68713|5|Briefly described|p19, p22|Middle Devonian|Middle Devonian|Newly identified. Detrital zircon dated marine sedimentary succession.  Youngest dates are Cambrian. K-Ar date based on the combined minimum age of 3 basaltic flows.|388 +/- 14 Ma, K-Ar||||Comprises a marine sedimentary succession with a more localised submarine basaltic volcanic member including some interflow clastics containing shelly fossils.|05-SEP-18
78310|Ooloo Hill Formation|69019|2|Defined|p15 Fig.4, p72-81, p146, p203-222, p230.|Devonian|Devonian|New name, after Ooloo Hill. Of Sheard and Wade (2012). Type drillhole: CRA Exploration RD/DD94WB3. Thickness >76m. Petrology and geochemistry are detailed with a stratigraphic section (Fig.15). Dating issues are discussed in detail.|388 +/- 14 Ma min. (whole-rock K-Ar).||||Laminated and massive shales, well-laminated or massive siltstone, intercalated sandstone beds; localised vesicular to massive basalt lavas and clastic sediments: sandstone to quartzite, arkose and greywacke, with interleaved polymict conglomerates.|
78310|Ooloo Hill Formation|75063|5|Briefly described|p91-95|Middle Devonian|Middle Devonian|NW of the Flinders Ranges; c.80km NE of Lyndhurst. Occupies a restricted <370 km2 basin below 280-300m of sedimentary Mesozoic cover. Drillcore graphic log and depositional regime. Photographs, photomicrographs. Geochronology (K-Ar), geochemistry results tabulated. Probably shallow-marine environment. Overlaps in age with Wana Karnu Group, as well as deposits in the Darling and Adavale Basins.|392 +/- 8 Ma (whole rock K-Ar).||||Comprises two components: a sedimentary sequence of shales, siltstones and sandstones; and a basalt-sedimentary member. Lithologies described in detail. Geochemistry described.|
75077|Oonartra Creek Formation|62993|4|Described|p3, 4,13-15,18, 21, 37,39, 40,43|Paleoproterozoic|Paleoproterozoic|Olary Domain.||Raven Hill Subgroup|||Coarse grained, sillimanite schist with a graphitic basal unit. Coarse grained aluminous schist with a basal graphitic unit. Banded quartz magnetite+ Mn garnet iron formation.|19-DEC-21
75077|Oonartra Creek Formation|63102|5|Briefly described|p14,32-34,58|Statherian|Statherian|Geological province: Olary Domain, Curnamona Province. Areally restricted to the western Kalabity Inlier. Underlain by a sequence of thin graphitic pelite, which is equivalent to Plumbago Formation.|c. 1695-1685 Ma|Unit of Saltbush Subgroup.||Equivalent to upper part of Broken Hill Group.||
75077|Oonartra Creek Formation|64741|5|Briefly described|p301 Fig. 4, p309|Paleoproterozoic|Paleoproterozoic|Of Raven Hill Subgroup (Saltbush Group). Geological province: Olary Domain. Contains manganiferous banded quartz-magnetite-grunerite-garnet iron formations and quartz-grunerite (coticule) rocks and occasional mafic sills.||||||07-FEB-11
75077|Oonartra Creek Formation|64944|5|Briefly described|p28 Fig. 1, p29 Tb. 1|Paleoproterozoic|Paleoproterozoic|Of Raven Hill Subgroup (Saltbush Group). Geological province: Olary Domain. Pelite and psammopelite with minor psammite layers and lenses.||||||07-FEB-11
75077|Oonartra Creek Formation|66302|6|Mentioned|p36 Fig.9, p39|Statherian|Statherian|Olary Domain, Curnamona Province. ||Raven Hill Subgroup||||
75077|Oonartra Creek Formation|70405|4|Described|p9 table 1, p28, p29, p41, p91, p96|Paleoproterozoic|Paleoproterozoic|Sedimentary exhalative chemical sediments suggestive of hydrothermal influence.||Raven Hill Subgroup||Overlies Black Maria Formation, intruded by Lady Louise Suite, correlated with (tentatively) Purnamoota Subgroup|Pyritic schist, pelites with thin psammite interbeds that are relatively coarse grained showing sharp bases and upward gradations to pelites.Sandstone and mudstone with graded bedding; Quartz-Mn garnet rocks and banded iron formations.|
75077|Oonartra Creek Formation|70657|4|Described|p14-15, p21, p33-34, p40-41, p44, p66|Statherian|Statherian|Conor (2004); modified to include the Broken Hill Group-type package above the Black Maria Formation. Curnamona Province, Olary Domain. Restricted to the western Kalabity Inlier. Mineralisation mentioned. May be prospective for Pb-Zn-Ag.|<1693 +/- 3 Ma  - >1655 Ma|Raven Hill Subgroup||Overlies Black Maria, George Mine and ?Plumbago Formations. ?Underlies Walparuta Formation. With Black Maria Formation is equivalent to Purnamoota Subgroup of Broken Hill Group (Broken Hill Domain).|Pelite, with occasional psammite layers, and characterised by manganiferous lenses of garnet quartzite, coticule and banded iron formation.|
75077|Oonartra Creek Formation|70658|5|Briefly described|p3, 7, 15|Paleoproterozoic|Paleoproterozoic|Olary Domain, Curnamona Province.||Raven Hill Subgroup.||Locally overlies Plumbago Formation.|Interbedded psammopelite, pelite and garnetiferous psammite.|
34793|Oorlano Metasomatite|22948|4|Described|p18|Mesoproterozoic|Mesoproterozoic|This rock is being developed commercially as an ornamental 'granite' known as "Harlequin Stone".||||||
34793|Oorlano Metasomatite|23981|5|Briefly described|p32|Precambrian|Precambrian|Forms basement rock on Yorke Peninsula overlain by Cambrian and Permian strata (including Coobowie Limestone, Moonan Formation and Stansbury Limestone) at Port Julia.||||||15-FEB-07
34793|Oorlano Metasomatite|24475|2|Defined|p56|Mesoproterozoic|Mesoproterozoic|||||||
34793|Oorlano Metasomatite|60958|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Geological Province: Gawler Craton. Metasomatic rocks of albite, scapolite. diopside, tremolite, epidote, carbonate, quartz, mica, magnetite.||||||14-APR-05
34793|Oorlano Metasomatite|61121|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Metasomatic rocks of albite, scapolite, diopside, tremolite, epidote, carbonate, quartz, mica, magnetite. Geological Province: Gawler Craton.||||||02-JUN-05
34793|Oorlano Metasomatite|65375|4|Described|p25.|Mesoproterozoic|Mesoproterozoic|Contains both Mesoproterozoic granite and Wallaroo Group protoliths. Related to hydrothermal systems during intrusion of Tickera Granite.|c.1585 Ma final metasomatic age.||||Series of metasomatic skarn-like rocks of calc-silicate, feldspar-rich and iron-rich composition; combinations of albite, microcline, scapolite, actinolite, diopside, tremolite, epidote, carbonate, quartz, biotite, magnetite and haematite.|
34793|Oorlano Metasomatite|65376|6|Mentioned|p101 Fig.3.1.|||||||||
34793|Oorlano Metasomatite|67536|5|Briefly described|Map Legend|Calymmian|Calymmian|Gawler Craton.|ca. 1586 +/- 5 Ma||||Alkali feldspar, iron-rich, carbonate and calcsilicate metasomatite.|
34793|Oorlano Metasomatite|69748|5|Briefly described|p179, 181, 183-190, 193-199|Mesoproterozoic|Mesoproterozoic|Conor (1995). Moonta-Wallaroo region, Olympic IOGC Province. Photomicrographs. REY fractionation trends graphed.|||||Calc-silicate feldspar schist; alternating bands dominated by either feldspars (both albite and K-feldspar) or calc-silicates (actinolite and clinozoisite).|
34793|Oorlano Metasomatite|73026|5|Briefly described|p9|Mesoproterozoic|Mesoproterozoic||||||Calc-silicate; feldspathic and iron rich metasomatite.|
34793|Oorlano Metasomatite|73027|5|Briefly described|p9,|Mesoproterozoic|Mesoproterozoic||||||Calcsilicate, feldspathic and iron rich metasomatite.|
34793|Oorlano Metasomatite|73092|5|Briefly described|p2-3, p33, p35-36, p39|Mesoproterozoic|Mesoproterozoic|Spectrum of ages obtained in this study were interpreted to be from detrital zircons. Maximum depositional ages range from c. 1863 Ma to c. 1755 Ma based on samples from Oorlano Quarry [also referred to as Harlequin stone quarry].|||||Skarn-like metasomatic rock dominated by feldspar, amphibole and pyroxene together with variable amounts of epidote, magnetite, biotite, carbonate, pyrite and chalcopyrite.|
34793|Oorlano Metasomatite|73103|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Is also shown in the Solid Geology Interpretation map, below the main Whyalla 250k map.|||||Calcsilicate; feldspathic and iron-rich metasomatite.|
34793|Oorlano Metasomatite|73644|5|Briefly described|p3|Mesoproterozoic|Mesoproterozoic|Collective term for alteration assemblages associated with the Hiltaba Suite on the Yorke Peninsula.||Hiltaba Suite|||Calc-silicate, feldspathic and iron-rich alteration assemblages.|
26090|Opaminda Formation|22869|6|Mentioned|P46|||Correlated to the Carey Gully Sandstone Member||||||
26090|Opaminda Formation|22889|6|Mentioned|p31|Adelaidean|Adelaidean|Parent - Emeroo Subgroup.  Former Parent - River Wakefield Subgroup, see p33 for details.||||||
26090|Opaminda Formation|23394|5|Briefly described|Map legend|Proterozoic|Proterozoic|||||||
26090|Opaminda Formation|23411|6|Mentioned|Map Legend|||||||||
26090|Opaminda Formation|23562|5|Briefly described|p295 Fig 2|Cryogenian|Cryogenian|||||||
26090|Opaminda Formation|24176|4|Described|p10, p25 Tb. 1|Adelaidean|Adelaidean|Of Callana Beds.  Dark grey siltstones, minor shale, magnesian dolomite.  Overlies Blue Mine Conglomerate.  Age is Willouran.  Max. thickness: 380m.  Type area near "Arkaroola".  Geological Province: Mount Painter Province.||||||
26090|Opaminda Formation|24546|5|Briefly described|p2 - 3 Fig.2|Neoproterozoic|Neoproterozoic|Of Burra Group. Overlain by River Wakefield Subgroup. Geological Province: Adelaide Fold Belt.||||||16-JAN-08
26090|Opaminda Formation|24593|5|Briefly described|p613 Fig. 1b|||Of the Burra Group.  Geological Province: Mount Painter Inlier.||||||
26090|Opaminda Formation|30176|6|Mentioned|Map legend|Adelaidean|Adelaidean|Willouran||||||
26090|Opaminda Formation|30177|2|Defined|p128|Adelaidean|Adelaidean|See also p63. Type section: North and south of Arkaroola track, 1.6 miles northwest of Arkaroola Homestead, lat. 30degrees 18'45"S long. 139degrees 21'07"E to lat. 30degrees 19'08"S long. 139degrees 20'57"E.||||||08-DEC-22
26090|Opaminda Formation|30801|6|Mentioned|p5|||Upper Callanna Beds. Table P5-6||||||
26090|Opaminda Formation|30807|6|Mentioned|p103|||Suggested map symbol||||||
26090|Opaminda Formation|32724|6|Mentioned|Fig.1|||Willouran. Correlation||||||
26090|Opaminda Formation|33474|6|Mentioned|Fig.4|||||||||
26090|Opaminda Formation|35255|6|Mentioned|Fig.7|||||||||
26090|Opaminda Formation|36733|6|Mentioned|Table 5|||||||||
26090|Opaminda Formation|37854|6|Mentioned|p14|||See Table 1.||||||
26090|Opaminda Formation|38157|6|Mentioned|Table III|||||||||
26090|Opaminda Formation|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Torrensian||||||
26090|Opaminda Formation|40294|6|Mentioned|Table 1|||||||||
26090|Opaminda Formation|41403|6|Mentioned|p43|||||||||
26090|Opaminda Formation|41404|4|Described|p93|||||||||
26090|Opaminda Formation|42222|6|Mentioned|p13|||||||||
26090|Opaminda Formation|43052|5|Briefly described|p177,Table 6.1|||of River Wakefield Subgroup||||||
26090|Opaminda Formation|61523|5|Briefly described|p12|Adelaidean|Adelaidean|Geological Province: Mount Painter Inlier.||||||
26090|Opaminda Formation|65379|5|Briefly described|p643, p644|Neoproterozoic|Neoproterozoic|Of Burra Group (Warrina Supergroup). Siltsone, dark-grey, well bedded; pale green talcose shale; amphibolite; marble. N.B. Asbestos deposit host, contains Bolla Bollana asbestos prospect.||||||07-MAR-12
26090|Opaminda Formation|65925|5|Briefly described|p124 Fig.3, pp125-126, Appendix 2.|||Subjected to low-grade (greenschist facies) metamorphism.||Unit in Burra Group.||Overlies Blue Mine Conglomerate. Is overlain by Wortupa Quartzite.|Siltstone, dark grey, well bedded; pale green talcose shale; amphibolite; marble.|
26090|Opaminda Formation|70384|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Adelaide Geosyncline. Age shown more specifically as Torrensian [Cryogenian].||Emeroo Subgroup.||Conformably? overlies Blue Mine Conglomerate. Is overlain conformably? by Wortupa Quartzite.|Dark grey, well-bedded siltstone; pale green talcose shale; amphibolite; marble.|18-JAN-19
26319|Ouldburra Formation|22613|4|Described|p17|Early Cambrian|Early Cambrian|Officer Basin||||||
26319|Ouldburra Formation|22614|5|Briefly described|map|Cambrian|Cambrian|||||||
26319|Ouldburra Formation|22650|6|Mentioned|p 159|Cambrian|Cambrian|Province - Officer Basin.||||||
26319|Ouldburra Formation|22746|5|Briefly described|Fig.3 p515|Early Cambrian|Early Cambrian|||||||
26319|Ouldburra Formation|22922|6|Mentioned|34|||||||||
26319|Ouldburra Formation|23054|6|Mentioned|p17||Early Cambrian|||||||
26319|Ouldburra Formation|23282|2|Defined|p70||Early Cambrian|of Brewer et al (1987). Age: Early Cambrian 536 - 524Ma. Of Marla Group, Officer Basin.||||||11-FEB-09
26319|Ouldburra Formation|23287|6|Mentioned|Fig.4|||Age: Lower Cambrian. of Eastern Officer Basin.||||||
26319|Ouldburra Formation|23288|6|Mentioned|Fig.5||Early Cambrian|||||||
26319|Ouldburra Formation|23524|5|Briefly described|p221 Fig. 3|Early Cambrian|Early Cambrian|||||||
26319|Ouldburra Formation|23981|5|Briefly described|p10 Fig. 5|Early Cambrian|Early Cambrian|Geological Province: eastern Officer Basin.||||||
26319|Ouldburra Formation|24112|5|Briefly described|p254 Fig.2, p268 Tb.5|Early Cambrian|Early Cambrian|Of the Marla Group. Geological Province: Officer Basin||||||
26319|Ouldburra Formation|40945|2|Defined|p8|Early Cambrian|Early Cambrian|||||||
26319|Ouldburra Formation|42065|5|Briefly described|p185|||See also Fig.2||||||
26319|Ouldburra Formation|42096|6|Mentioned|p37|||||||||
26319|Ouldburra Formation|42816|3|Fully described|p15|||||||||
26319|Ouldburra Formation|43657|6|Mentioned|Fig.3,p4||Cambrian|||||||
26319|Ouldburra Formation|43690|6|Mentioned|Fig.2,p157||Cambrian|||||||
26319|Ouldburra Formation|43732|5|Briefly described|p3|||||||||
26319|Ouldburra Formation|43743|6|Mentioned|Fig.2,p33||Early Cambrian|||||||
26319|Ouldburra Formation|44109|5|Briefly described|p22 Fig. 19|Cambrian|Cambrian|Of the Marla Group. Geological Province: central Officer Basin.||||||
26319|Ouldburra Formation|44133|5|Briefly described|p4 Fig. 7.2, 9 Fig. 7.5, 35|Early Cambrian|Early Cambrian|Geological Province: Eastern Officer Basin. Of the Marla Group. Maximum Thickness at Type section: 1114m.||||||
26319|Ouldburra Formation|44695|5|Briefly described|Map Legend||Cambrian|||||||
26319|Ouldburra Formation|60565|5|Briefly described|p18, p20 Fig. 3b|Cambrian|Cambrian|Carbonates and thick salt deposits; largely dolomite. Geological Province: Manya and Tallaringa Troughs.||||||16-JUN-05
26319|Ouldburra Formation|61732|5|Briefly described|p67|Cambrian|Cambrian|Of the Marla Group. Fossiliferous unit.||||||07-FEB-11
26319|Ouldburra Formation|62570|4|Described|p579, p580 Figs. 2 and 3|Early Cambrian|Early Cambrian|Of Marla Group. Conformably overlain by Observatory Hill Formation. Main part - thick limestone-dolostone units; lower part - cyclic suite of halite-carbonate-siliciclastic units. Salt is up to 5m thick. Geological Province: Officer Basin.||||||01-OCT-09
26319|Ouldburra Formation|64159|5|Briefly described|p94|Cambrian|Cambrian|Geological Province: Officer Basin. Includes saddle dolomite in dolomitised limestones.||||||
26319|Ouldburra Formation|64794|6|Mentioned|p238 fig 2|Early Cambrian|Early Cambrian|||||||
26319|Ouldburra Formation|64813|5|Briefly described|p272|Early Cambrian|Early Cambrian|Geological province: Officer Basin, S.A. Limestone deposits laid down in a shallow epeiric sea.||||||
26319|Ouldburra Formation|65313|5|Briefly described|p577|Early Cambrian|Early Cambrian|Officer Basin. Manya 6 well.  Age: (mid-late Atdbanaian, Abadiella officerensis zone), based on trilobites.|ca 520 Ma.|||||26-MAR-12
26319|Ouldburra Formation|65686|6|Mentioned|p412|Early Cambrian|Early Cambrian|East Officer Basin.|||||Siltstone.|07-MAY-12
26319|Ouldburra Formation|67344|6|Mentioned|p264 Tb.3|Cambrian|Cambrian|Of the Officer Basin. Unmetamorphosed Cambrian series 2 formation. Shallow-water marine carbonate deposit; benthic cyanobacteria in its sabkha paleoenvironment. Bulk organic carbon isotopic composition almost identical with Emu Bay Shale.||||||
26319|Ouldburra Formation|67536|6|Mentioned|Map Legend|||One of several Formations mapped collectively as Em4.|||||Marine limestone and dolomite.|01-APR-14
26319|Ouldburra Formation|69648|4|Described|p19, p34-36, map legend|Early Cambrian|Early Cambrian|Of Brewer et al. (1987). In northeastern Office Basin. Tallaringa Trough. Unit occurs in drillholes on adjacent map sheets and may extend into northeastern OOLDEA. Sequence of mixed carbonate/siliciclastics, marine carbonates and evaporites, mainly in drillholes on BARTON and TALLARINGA. A 594 m thick section in drillhole Wilkinson l on adjacent TALLARINGA was originally referred to as Observatory Hill Beds, but Brewer et al. (1987) correlated these sediments with Ouldburra Formation. The lower Ouldburra Formation is a suite of halite-siliciclastic and halite-carbonate-siliciclastic rocks, indicative of a mosaic of isolated salinas on a shallow marine to exposed sandy mudflat bordered by aeolian dunes. Prospective for evaporite minerals.|Minimum: ~507 Ma|Marla Group||Relief Sandstone underlies. Boundary transitional.|Sediments, evaporite minerals; calcareous mudstone with gypsum and anhydrite, minor interbeds of very fine and coarse-grained sandstone, and laminated carbonaceous mudstone.|17-FEB-15
26319|Ouldburra Formation|69946|6|Mentioned|p38|||||||Conformably overlies Relief Sandstone. Is overlain conformably by Observatory Hill Formation.||
26319|Ouldburra Formation|70833|5|Briefly described|p203|Cambrian|Cambrian|Of Officer Basin. Contains few early Cambrian shelly fossils, described from Manya-6 drill core. Coeval with Reeeif Sandstone; broadly coincident with Hawker Group.||||||
26319|Ouldburra Formation|71342|6|Mentioned|Ch5 p38|Cambrian|Cambrian|Arckaringa Basin.||||Overlies the Relief Sandstone. Overlain by the Observatory Hill Formation.||
26319|Ouldburra Formation|72429|6|Mentioned|p972|Cambrian|Cambrian|Officer basin. Potentially Botoman in age? Shows evidence of anhydrite, potentially showing an intertidal estuarine sabkha to supratidal continental sabkha depositional environment.||||||
26319|Ouldburra Formation|72478|6|Mentioned|p8|Early Cambrian|Early Cambrian|Officer Basin.|c. 536-524 Ma|Marla Group||||25-MAR-21
80367|Outalpa Quartzite Member|70657|5|Briefly described|p22, p25|||Suggested in this study that this name, a modification of the Outalpa Quartzites of Campana and King (1958), be applied to the lower part of the Tommie Wattie Formation.||Tommie Wattie Formation.|||Clean, pale brown metasandstones.|
31512|Overland Corner Clay Member|23226|2|Defined|p900||Balcombian|Age: due to lateral equivalence to Murbko Marl Member and its strat position. Lithologically similar to Cowirra Clay Member. Of Cadell Formation.||||||
31512|Overland Corner Clay Member|64237|5|Briefly described|p19 Fig. 2b|Middle Miocene|Middle Miocene|Of Cadell Formation (Morgan Subgroup, Murray Group); introduced as member of the Morgan Group (Murray Supergroup) by Lukasik and James (1998) and retained as a member of the Cadell Formation of the new Morgan Subgroup..........Geol.Province: Murray Basin.||||||29-JUL-08
76222|Pack Creek Member|72429|4|Described|p952, p956, p971-972|Lower Cambrian|Lower Cambrian|Mount Chambers Gorge, eastern Flinders Ranges. Up to 46m thick in measured section. Conglomerate clasts are discussed further, including their origin, size, shape and formation.||Moorowie Formation||Overlies the Kandramooka Member. Underlies the Brillig Catch Member.|Purple-red micaceous siltstone with thin grey limestone laminations at base. Local thin polymict conglomerate lenses with light grey limestone cobbles and quartz granule-carbonate pebbles in a silty lime matrix.|
83693|Padthaway Ridge suite|73430|6|Mentioned|p495|Middle Ordovician|Late Cambrian|Post-tectonic A-type magmatic series (Turner et al., 1992). Occurs as scattered outcropping inliers in the Murray Basin. Dated samples include the granite at Kongal Rocks (486.1+/-1 Ma). May include an undeformed granodiorite from drill hole PADD28 with a LA-ICP-MS zircon U-Pb age of 475.2+/-1 Ma. See also variations 'Padthaway Ridge' series p495, Padthaway A-type granite suite p498, Padthaway Ridge A-type granite p496 Fig.4, p500, p502, p507, Padthaway Ridge A-type suite p518.  [Misspelt as Pathaway p498]|486.1+/-1 Ma, 470.1+/-1 Ma LA-ICP-MS zircon U-Pb||Mannum Granite, Marcollat Granite, Monteith Granite, Mount Monster porphyry/Mount Monster rhyolite.||Includes undeformed, potassium rich granite.|
38564|Paling Formation|24396|4|Described|p222|Eocene|Eocene|Formerly Paling Member of the Wilson Bluff Limestone.||||||
38564|Paling Formation|24397|3|Fully described|p238|Middle Eocene|Middle Eocene|Formerly Paling Member of Wilson Bluff Limestone. Overlain by Pidinga Formation; underlain by Maralinga Formation.  Geological Province: Eucla Basin.||||||15-APR-09
38564|Paling Formation|24606|6|Mentioned|p957 Fig. 2|||Geological Province: Eucla Basin. Formation is Fm in text.||||||
38564|Paling Formation|24617|6|Mentioned|p114, p115 Fig. 3, p119, p125 Fig. 10|Eocene|Eocene|Geological Province: Eucla Basin.||||||15-APR-09
38564|Paling Formation|61234|4|Described|p6, p7 Fig. 4|Middle Eocene|Middle Eocene|Geological Province: Eucla Basin. Overlain by Khasta Formation. Lagoonal carbonaceous limestone.||||||14-MAY-07
38564|Paling Formation|64646|6|Mentioned|p23 Fig. 3|Eocene|Eocene|Geological Province: Gawler Craton.||||||08-FEB-10
38564|Paling Formation|67462|5|Briefly described|Map legend.|Eocene|Eocene|Eucla Basin.||||||
38564|Paling Formation|68715|6|Mentioned|p30 Fig.5|Bartonian|Bartonian|SW Gawler Craton, Eucla Basin.||||||
38564|Paling Formation|69598|6|Mentioned|p9|||||||||
28186|Palthrubie Granophyre|30984|2|Defined|p10|Proterozoic|Proterozoic|||||||
28186|Palthrubie Granophyre|41974|5|Briefly described|Table 1 P412|||||||||
22621|Pando Formation|13497|6|Mentioned|p96, p114|||Warburton Basin.||||||
22621|Pando Formation|22527|6|Mentioned|p 5|||||||||
22621|Pando Formation|23154|5|Briefly described|Map Legend|Cambrian|Cambrian|Geological Province - Warburton Basin.||||||
22621|Pando Formation|23155|2|Defined|p7 & Fig 3|Early Cambrian|Early Cambrian|Type section location advised p7.  Age - presumed to be Early Cambrian on the basis of penetrative burrows resembling Chondrites.  Geological Province - eastern Warburton Basin.||||||01-APR-14
22621|Pando Formation|24482|5|Briefly described|p44|Ordovician|Cambrian|Geological Province: Warburton Basin.||||||
22621|Pando Formation|43052|5|Briefly described|Table 2.1|||||||||
22621|Pando Formation|43201|6|Mentioned|p8|||||||||
22621|Pando Formation|44133|5|Briefly described|p4 Fig. 7.2, 31|Early Cambrian|Early Cambrian|Geological Province: Eastern Warburton Basin. Underlies and intertongues with Mooracoochie Volcanics.||||||01-APR-14
22621|Pando Formation|62537|6|Mentioned|p191 Fig.2. |Ordovician|Late Cambrian|Warburton Basin.||||||
22621|Pando Formation|63056|5|Briefly described|p80, p81 Fig. 2|Early Cambrian|Early Cambrian|Extensive marine shelf. Equivalent to the lower Innamincka Formation. Thickness: 240m. Geological Province: Warburton Basin. Bioturbated glauconitic 'hot' sandstone, good reservoir properties. See also p82.||||||06-FEB-07
22621|Pando Formation|63978|5|Briefly described|p5|Early Cambrian|Early Cambrian|Interfingers with overlying Mooracoochie Volcanics. Geological province: Warburton Basin.||||||07-FEB-11
22621|Pando Formation|65489|5|Briefly described|p15, p28-29, p37, p39, p96, p119-121|Early Ordovician|Late Cambrian|Gatehouse et al. (1995). Eastern Warburton Basin. Good reservoir properties: 5-20% porosity, but relies on fractures for permeability. Zircon-rich: has high gamma ray response. Hosts Moolalla 1 gas.||||Overlies Kalladeina Formation. Is overlain by Innamincka Formation.|Clean quartzose sandstone to bioturbated glauconitic sandstone; interbedded siltstone and shale.|
22621|Pando Formation|65925|5|Briefly described|Appendix 2.||||||||Sandstone, pale green-grey, laminated, bioturbated, silty. With glauconite.|
22621|Pando Formation|67402|4|Described|p239, p261|Lancefieldian|Lancefieldian|Warburton Basin. Unsuitable reservoir for the storage of carbon dioxide. Deposited in a marine shelf. 246m thick. ||||Overlies the Kalladeina Formation. Overlain by the Dullingari Group. Grades laterally into the Innamincka Formation.|Dominantly bioturbated and glauconitic 'hot' sands.|
22621|Pando Formation|67536|6|Mentioned|Map Legend|||Warburton Basin.|||||Glauconitic sandstone.|01-APR-14
22621|Pando Formation|68731|5|Briefly described|p168, p170 Fig 3.83|Early Cambrian|Early Cambrian|~ 240 m thick. Bioturbated glauconitic 'hot' sandstone, gas in Moolalla/(?low stand wedge), good reservoir properties.||||Partly underlain by the Kalladeina Formation.|Contains shale, sandstone, and siltstone.|
22621|Pando Formation|69019|6|Mentioned|p145-146.|||Warburton Basin. Sub-vertical.||||Intruded by Big Lake Suite granite.||
22621|Pando Formation|69023|5|Briefly described|p82, p85, p149|Early Cambrian|Early Cambrian|Warburton Basin. Sub-vertical rocks intruded by granites of Big Lake Suite. Source of reworked glauconite for overlying Merrimelia Formation.||||Is overlain by Merrimelia Formation. Is intruded by Big Lake Suite.||
22621|Pando Formation|69982|1|Redefined|p29-31, p10,p13, p17-19, p23, p38-39,p45|Early Ordovician|Early Ordovician|See also p51-55, p143-144, p153, p220, p223-224, Appendix 1. Gravestock (1995), referring to a bioturbated glauconitic sandstone unit with abundant heavy minerals, which had previously been part of the Dullingari Group (Gatehouse, 1983). Type section is the interval 1736 - 1933 m in Pando 1. Excludes the thick shale of the Lycosa Formation, and the ignimbrite of the Mooracoochie Volcanics, in the original definition. Includes an orthoquartzite previously believed to be  'of possibly Proterozoic age' (Gravestock, 1995) found in some Daralingie wells. Warburton Basin. c.240 m thick. Age and stratigraphic relationships unclear. Hosts 32%  of the oil, and 12% of gas, shows in the Basin: produces gas in Moolalla 1 well. Three lithofacies detailed. Reservoir attributes described. Brief thin section descriptions. Composite logs shown. Bedding dip angles in wells listed. Details of wells with hydrocarbon shows.||||Unconformably overlies Lycosa Formation.|Clean bioturbated, fine- to coarse-grained glauconitic quartzose sandstone containing abundant zircons; minor interbedded thin, brownish-grey, micaceous siltstone and shale.|12-NOV-15
22621|Pando Formation|70749|6|Mentioned|p54|||Warburton Basin. Shoreline deposits.||||||
22621|Pando Formation|73244|6|Mentioned|p86|Ordovician|Ordovician|Warburton Basin. Lowstand fan environment. Gas.||||||
22621|Pando Formation|73479|5|Briefly described|p156 Fig.2, p157|Ordovician|Cambrian|Warburton Basin. Lowstand fan depositional environment.|ca 488 Ma|||Overlies Kalladeina Formation, underlies Innamincka Formation||
36783|Paney Rhyolite Member|24346|3|Fully described|p104, p111 App 1.|||Of Eucarro Rhyolite. Formerly Paney Rhyolite and "Paney Rhyolite"|||||Heterogeneous. Compositionally and texturally distinct flow bands of: orange-buff, find grained quartz-rich rhyolite; mottled green and vesicular rhyolite;  red, coarse-grained + plagioclese-rich rhyolite.|20-MAR-15
36783|Paney Rhyolite Member|70659|5|Briefly described|p8|Mesoproterozoic|Mesoproterozoic|Gawler Ranges.||Eucarro Rhyolite.||||
36783|Paney Rhyolite Member|70816|5|Briefly described|p5|||Gawler Ranges region.||Unit of Eucarro Rhyolite||Uppermost unit of Eucarro Rhyolite. Underlain by Yannabie and Nonning Rhyolite Members.||
36783|Paney Rhyolite Member|71317|4|Described|p1, p20, p39-p44, p54-p60|Mesoproterozoic|Mesoproterozoic|Previously the Paney Rhyolite. Petrography discussed in some detail. Referred to as the Paney Rhyolite on p57-p58. See also p68, p70, p84, p191.||Eucarro Rhyolite||Overlies the Yannabie Rhyolite Member. Disconformably overlain by the Mount Friday Formation.|Yellowish-orange to reddish-brown, locally buff-coloured or pale greenish porphyritic rhyolite with phenocrysts of quartz and feldspar in a fine-grained groundmass.|
36783|Paney Rhyolite Member|71559|4|Described|p16-p17, p19, p22|Mesoproterozoic|Mesoproterozoic|Geological province: Gawler Craton.||Unit of Upper Gawler Range Volcanics.||Underlain by Eucarro Rhyolite.|Rhyolite, red, porphyritic with phenocrysts of quartz and feldspar, commonly flow-banded, locally mingled wih Eucarro Rhyolite at base.|19-JUN-19
36783|Paney Rhyolite Member|71560|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|||Eucarro Rhyolite.|||Rhyolite, red, amygdaloidal and porphyritic with phenocrysts of quartz and feldspar, commonly flow-banded; locally mingled with Eucarro Rhyolite at base.|
36783|Paney Rhyolite Member|72065|5|Briefly described|p105,108,112,115|Calymmian|Calymmian|Geological province: Gawler Craton. Interfingers with feldspar-phyric rhyolite assemblages of the parent Eucarro Rhyolite.||Unit of Eucarro Rhyolite.||||
36783|Paney Rhyolite Member|72090|6|Mentioned|p12|||Gawler Craton.||Eucarro Rhyolite||||
36783|Paney Rhyolite Member|73110|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|||Eucarro Rhyolite.|||Rhyolite, fine- to coarse-grained, porphyritic, commonly flow-banded. Near Conflagration Dam contains large lithic clasts.|
23892|Paning Member|13497|4|Described|iv, vi, viii, xii, p69 fig 6.1|Anisian|Scythian|Cooper Basin.This member was initialtly defined by Powis (1989) however it was subsequently redefined by Channon and Wood (1989). Three reference sections are mentioned, including one from Powis (1989) and two from Channon and Wood (1989). Petrography discussed in detail. Distribution is briefly discussed. More than 200m thick in the Moomba Field where it has been drilled. Outcrop and reservoir characteristics discussed. See also p104-p105, p108-p110, p157 tbl 10.1 , p159, p161, p166, p172.||Arrabury Formation||Disconformably overlies the Callamurra Member. Overlain by and is equivalent to, the Wimma Sandstone Member.|Upwards-fining cycles of buff, pale grey to off white, fine to medium-grained sandstone grading into light to dark grey and brown siliceous mudstone and siltstone.|
23892|Paning Member|22883|6|Mentioned|P29|||Parent is Arrabury Formation||||||
23892|Paning Member|23155|6|Mentioned|Fig 8 on p16|||Age - Triassic?||||||
23892|Paning Member|23375|4|Described|Fig2 p265,280|Nammalian|Griesbachian|Of the Arrabury Formation, Cooper Basin.||||||17-JAN-08
23892|Paning Member|24210|5|Briefly described|p133 Fig. 2|Middle Triassic|Early Triassic|Of the Arrabury Formation (Nappamerri Group).  Geological Province: Cooper Basin.||||||
23892|Paning Member|24372|6|Mentioned|p21|||Geological Province: Cooper Basin.||||||
23892|Paning Member|42008|3|Fully described|PP270|Scythian|Tatarian|Of the Arrabury Formation.||||||17-JAN-08
23892|Paning Member|42085|6|Mentioned|Fig.2 P374|||||||||
23892|Paning Member|44133|5|Briefly described|p65 Fig. 8.3, 86|Triassic|Triassic|Of the Arrabury Formation. Geological Province: Cooper Basin. Overlies: Callamurra Member (u).||||||
23892|Paning Member|60717|5|Briefly described|p40 Fig. 2|Scythian|Scythian|Of Arrabury Formation (Nappamerri Group). Overlies Callamurra Member and part of Paning Member of the same unit. Thickness: 150m. Geological Province: Cooper Basin.||||||31-JAN-08
23892|Paning Member|61613|5|Briefly described|p282 Fig. 2|Early Triassic|Late Permian|Of Arrabury Formation. Overlain by Wimma Sandstone Member, Underlain by Callamurra Member. Geological Province: Cooper and Simpson Basins.||||||26-JUN-14
23892|Paning Member|61615|6|Mentioned|p302 Fig. 2|Middle Triassic|Early Triassic|Of Nappamerri Group. Geological Province: Cooper Basin.||||||07-FEB-11
23892|Paning Member|61616|6|Mentioned|p330 Fig. 2|Early Triassic|Early Triassic|Of Arrabury Formation. Geological Province: Cooper Basin.||||||31-MAR-09
23892|Paning Member|62730|5|Briefly described|p352 Fig. 1|Early Triassic|Early Triassic|Of the Arrabury Formation. Geological Province: Cooper Basin.||||||21-APR-08
23892|Paning Member|63978|2|Defined|p21, Fig. 3|Early Triassic|Early Triassic|Of Arrabury Fm. Paning Mbr originally included Callamurra Mbr also (Powis 1989); then redefined by Gary (2000) interpreting the Callamurra Mbr conformably below Paning Mbr. Conformable below Wimma Sst Mbr. Max. thick: 200m. Detailed lithology included.||||||07-FEB-11
23892|Paning Member|64048|5|Briefly described|p66|||Within the Middle Arrabury Formation. Directly overlies the Callamurra Member. Contains considerable amounts of interbedded sandstones which contain commercial quantities of gas.||||||07-FEB-11
23892|Paning Member|64197|6|Mentioned|p625 Fig.1c|Early Triassic|Early Triassic|Cooper Basin||Unit in Arrabury Formation||Overlies Callamurra Member. Is overlain by Wimma [Sandstone] Member.||
23892|Paning Member|64665|5|Briefly described|p53 Fig.2.|Early Triassic|Early Triassic|Cooper Basin.||Middle unit in Arrabury Formation.||Is overlain by Wimma Sandstone Member.||
23892|Paning Member|65489|5|Briefly described|p48, p96, p131-132|Scythian|Scythian|150m thick. Hosts economic oil and gas reservoirs.||Unit in Arrabury Formation.||Overlies Callamurra Member. Is overlain by Wimma Sandstone Member.||
23892|Paning Member|67402|5|Briefly described|p90 fig CPR4|||Misspelt as the Panning Member on p91. Probably a facies equivalent of the Wimma Sandstone Member. Maximum thickness of 150m. See also p91 tbl CPR1, p90-p94, p101, p101 tbl CPR2, p105.||Arrabury Formation||Conformably (or mildly unconformably) overlies the Callamurra Member. Conformably overlain by the Wimma Sandstone Member.|Fine to medium-grained sandstones and siltstones that fine upwards.|
23892|Paning Member|68731|5|Briefly described|p200 Fig 3.110, p207|Middle Triassic|Early Triassic|Cooper Basin. Strata that Powis (1989) assigned to the lower Paning Member is now included in the Callamurra Member.||Of the Arrabury Formation.||Underlain by the Callamurra Member (possible disconformity). Conformably overlain by the Wimma Sandstone Member.||
23892|Paning Member|69797|5|Briefly described|p17 Fig.2|Early Triassic|Early Triassic|Age: Scythian (approximated from figure). Geol. Prov: Cooper Basin.||Arrabury Formation||||
23892|Paning Member|69946|5|Briefly described|p9, p36, p54|Scythian|Scythian|Cooper Basin.||Unit in Arrabury Formation.||Overlies Callamurra Member. Is overlain by Wimma Sandstone Member.||
23892|Paning Member|69947|5|Briefly described|p13 Fig.7.2|Middle Triassic|Early Triassic|Cooper Basin.||Arrabury Formation.||||
23892|Paning Member|70317|6|Mentioned|p33|Early Triassic|Early Triassic|Cooper Basin.||Arrabury Formation.||Overlies Callamurra Member. Is overlain by Wimma Sandstone Member.||
23892|Paning Member|70823|5|Briefly described|p40, p75, p79, p81|||Cooper Basin. Contains economic oil and gas reservoirs locally.||Arrabury Formation||Overlain by the Wimma Sandstone Member.|Thin fine to medium grained quartzose sandstones.|
23892|Paning Member|70824|4|Described|p7, p104|Olenekian|Olenekian|Cooper Basin. Deposited in braided fluvial channels and floodplain environments.||Arrabury Formation||Unconformably overlies the Callamurra Member. Conformably overlain by the Wimma Sandstone Member.|Basal mudstone and siltstone with thin fine to medium-grained quartzose sandstone interbeds.|
23892|Paning Member|70946|5|Briefly described|p1089|Early Triassic|Early Triassic|Cooper Basin. Deposited in a braided fluvial channel belt and floodplain environment.||Arrabury Formation.||Unconformably overlies the Callamurra Member.||08-OCT-18
23892|Paning Member|71265|5|Briefly described|p589|Olenekian|Olenekian|Cooper Basin.||Arrabury Formation.||Overlies Callamurra Member.||
23892|Paning Member|71342|6|Mentioned|Ch5 p9, Ch5 p36, Ch5 p54, Ch7 p13|Anisian|Scythian|Cooper Basin. Palynological zone is given in fig 5.3 Ch5 p36. Deposited in a braided fluvial channel or floodplain environment.||Arrabury Formation||Overlies the Callamurra Member. Overlain by the Wimma Sandstone Member.||
23892|Paning Member|71701|5|Briefly described|p155|Olenekian|Olenekian|Cooper Basin.||Arrabury Formation||Unconformably overlies the Callamurra Member.||
23892|Paning Member|73251|6|Mentioned|p62|Early Triassic|Early Triassic|Cooper Basin. Braided fluvial channel belt and floodplain depositional environments. Contains[?] gas and oil.||Arrabury Formation, Nappamerri Group||Underlain by Callamurra Member. Overlain by and equivalent to Wimma Sandstone Member.||
25378|Pantapinna Sandstone|22766|5|Briefly described|Fig.2 p561|Middle Cambrian|Middle Cambrian|||||||
25378|Pantapinna Sandstone|22857|5|Briefly described|p90 Fig. 14.7B|Early Ordovician|Early Ordovician|Of the Lake Frome Group. Geological Province: Arrowie Basin. ||||||
25378|Pantapinna Sandstone|22858|6|Mentioned|Fig14.7bp90-1|||||||||
25378|Pantapinna Sandstone|23818|5|Briefly described|p87 Fig.33|Cambrian|Cambrian|Of the Lake Frome Group.||||||
25378|Pantapinna Sandstone|24072|5|Briefly described|p369 Fig.1|Cambrian|Cambrian|Geological Province: Great Artesian Basin.||||||
25378|Pantapinna Sandstone|24176|4|Described|p17, p23 Tb. 1|Late Cambrian|Late Cambrian|Of the Lake Frome Group.  Red and white feldspathic sandstone, minor silty sandstone.  Overlain by Grindstone Range Sandstone; underlain by Balcoracana Formation.  Max. thickness: 305m.  Geological Province: Mount Painter Province.||||||
25378|Pantapinna Sandstone|24465|5|Briefly described|p345 Fig.2|Middle Cambrian|Early Cambrian|Of Lake Frome Group.  Geological Province: Arrowie Basin.||||||19-JAN-05
25378|Pantapinna Sandstone|30176|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
25378|Pantapinna Sandstone|30801|6|Mentioned|p5|||Lake Frome Group. Table P5-6||||||
25378|Pantapinna Sandstone|30802|5|Briefly described|p11|||Cambrian age||||||
25378|Pantapinna Sandstone|30807|6|Mentioned|p102|||Suggested map symbol||||||
25378|Pantapinna Sandstone|33474|6|Mentioned|Fig.3|||||||||
25378|Pantapinna Sandstone|33932|6|Mentioned|Fig.2|||||||||
25378|Pantapinna Sandstone|33934|6|Mentioned|Fig.2|||M - U Camb.||||||
25378|Pantapinna Sandstone|33973|6|Mentioned|Fig.2|||||||||
25378|Pantapinna Sandstone|34269|6|Mentioned|Table 1|||||||||
25378|Pantapinna Sandstone|34610|6|Mentioned|p178|||Refers Dalgarno & Johnson (1965)||||||
25378|Pantapinna Sandstone|34612|6|Mentioned|p95|||Cambrian. Correlation chart Fig.33||||||
25378|Pantapinna Sandstone|35255|6|Mentioned|Fig.8|||||||||
25378|Pantapinna Sandstone|36198|6|Mentioned|Fig.I.2|||||||||
25378|Pantapinna Sandstone|38701|6|Mentioned|p123|||||||||
25378|Pantapinna Sandstone|40852|6|Mentioned|Fig.3.7|||||||||
25378|Pantapinna Sandstone|40914|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
25378|Pantapinna Sandstone|42090|5|Briefly described|p26|||||||||
25378|Pantapinna Sandstone|42222|6|Mentioned|Table 1 P5|||||||||
25378|Pantapinna Sandstone|42225|6|Mentioned|Fig.4 P224|||||||||
25378|Pantapinna Sandstone|42440|6|Mentioned|Fig.2 P602|||||||||
25378|Pantapinna Sandstone|43781|6|Mentioned|p4|||||||||
25378|Pantapinna Sandstone|43845|6|Mentioned|Fig4 p44|||||||||12-JUL-16
25378|Pantapinna Sandstone|44133|4|Described|p30, 4 Fig. 7.2, 28|Middle Paleozoic|Early Paleozoic|Geological Province: Arrowie Basin. Maximum Thickness: 1300m. Conformably overlies: Balcoracana Formation.||||||07-NOV-08
25378|Pantapinna Sandstone|60889|4|Described|p245 Fig.2, p247 Fig.4, p249, p252-4|Middle Cambrian|Middle Cambrian|Highstand deposits; marginal marine at base and probably of fluvial origin towards top. Thickness: 1400 m. Lithology continued: sandstones near top may lack effective regional seal. The lower Pantapinna Sandstone is considered to consist of stacked delta distributary sands. Arrowie Basin. Shown as Pantapinna Sst.||Lake Frome Group||Overlies Balcoracana Formation. Is overlain by Grindstone Range Sandstone.|Planar to trough cross-bedded fine to medium sandstone, minor siltstone and shale. Shaly intervals at top of upward-fining cycles.|
25378|Pantapinna Sandstone|60959|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of the Lake Frome Group.  Red and white feldspathic, medium-grained sandstone with minor micaceous siltstone and shale.||||||
25378|Pantapinna Sandstone|62592|5|Briefly described|p50 Table 5.1.|Early Cambrian|Early Cambrian|Adelaide Geosyncline.||Unit in Lake Frome Group.||Overlies Balcoracana Formation. Is overlain by Grindstone Range Sandstone.|Redbeds.|
25378|Pantapinna Sandstone|63569|5|Briefly described|p117 Fig.1|Middle Cambrian|Middle Cambrian|Arrowie Basin. Thickness 1400 m.||Unit in Lake Frome Group.||||
25378|Pantapinna Sandstone|64829|5|Briefly described|p1084-5 Figs.1,  2|Late Cambrian|Middle Cambrian|Unit discussed in the context of soilscapes and palaeosols. Geological province: Arrowie Basin. Has associated palaeosols.||||||07-FEB-11
25378|Pantapinna Sandstone|65313|5|Briefly described|p576, Fig.5, p578 Fig. 6, p573 Fig. 2|Late Cambrian|Middle Cambrian| Age shown as Merionethian (Avalonian regional time scale). Paleocurrents to N and E indicate Gawler Craton as source terrane.||Of Lake Frome Group.||Underlies Grindstone Range Sandstone, overlies Balcoracana Formation.||26-MAR-12
25378|Pantapinna Sandstone|65375|5|Briefly described|p33.|Middle Cambrian|Middle Cambrian|||Unit in Lake Frome Group.||Ovelies Balcoracana Formation. Is overlain by Grindstone Range Sandstone.||
25378|Pantapinna Sandstone|65686|5|Briefly described|p409 Fig 2|Middle Cambrian|Middle Cambrian|Arrowie Basin. 1400m thick.||||||07-MAY-12
25378|Pantapinna Sandstone|65892|5|Briefly described|p7 Fig.3, p9 Fig.4, p11, p49.|Middle Cambrian|Middle Cambrian|Arrowie Basin. 1400m thick. Highstand deposits. Marginal marine at base, probably of fluvial origin towards the top.||Unit in Lake Frome Group.||Overlies Balcoracana Formation. Is overlain by Grindstone Range Sandstone.|Planar to trough cross-bedded, fine to medium sandstone with minor siltstone and shale.|
25378|Pantapinna Sandstone|65925|5|Briefly described|p14 Fig.2.2, Appendix 2.|Middle Cambrian|Middle Cambrian|||Unit in Lake Frome Group.|||Red, white, fine- to medium-grained feldspathic sandstone; minor micaceous siltstone and shale.|
25378|Pantapinna Sandstone|66518|6|Mentioned|p19 Fig.4.|Cambrian|Cambrian|Arrowie Basin. ||Unit in Lake Frome Group.||Overlies Balcoracana Formation and is overlain by Grindstone Range Sandstone.||
25378|Pantapinna Sandstone|68735|4|Described|p233 Fig.2, p235-238|Middle Cambrian|Middle Cambrian|Arrowie Basin. ~ 1400 m thick. Suggested marginal marine to fluviatile origin but with some open marine horizons. Cross-bedding rose diagrams. Paleocurrent measurements from Prism Hill (Stock 1974) indicate a flow direction towards the northeast.||Of the Lake Frome Group.||Underlain by the Balcoracana Formation. Overlain by the Grindstone Range Sandstone.|Comprises mainly fine to medium-grained feldspathic sandstones with minor siltstones and shales. Planar and trough cross-bedding is common.|10-APR-17
25378|Pantapinna Sandstone|68993|5|Briefly described|p543, p544 Fig.1|Middle Cambrian|Middle Cambrian|Arrowie Basin. Marginal marine to fluviatile origin, but with some open marine horizons.||Of the Lake Frome Group.||||
25378|Pantapinna Sandstone|69570|6|Mentioned|p421 fig 1|Cambrian|Cambrian|Arrowie Syncline, Flinder Ranges.||||||
25378|Pantapinna Sandstone|72449|5|Briefly described|p2 Map legend|Cambrian|Cambrian|Shown in image on p1, 'Work burroughs in the Parachilna Formation' ( photo 042163).||||Overlies Balcoracana Formation and underlies Grindstone Range Sandstone.|Reddish, medium-grained sandstone with minor mica-rich siltstone and shale; heavy mineral laminae; planar lamination and cross-bedding.|
25378|Pantapinna Sandstone|73251|6|Mentioned|p36|Cambrian|Cambrian|Arrowie Basin, Moorowie and Yalkalpo Sub-basins. Thermally late to post-mature. Potential hydrocarbon reservoir and fairway.||Lake Frome Group||Underlain by Balcoracana Formation. Overlain by Grindstone Range Sandstone.||
25378|Pantapinna Sandstone|73255|6|Mentioned|p534 Fig.2|late Cambrian|middle Cambrian|||||Overlies the Balcoracana Formation, underlies the Grindstone Range Sandstone.||
25694|Parakeelya Alkali Member|22613|6|Mentioned|p17|Neoproterozoic|Neoproterozoic|||||||
25694|Parakeelya Alkali Member|22922|6|Mentioned|33 fig 2|||Of Observatory Hill Formation, Officer Basin. Oil show.||||||
25694|Parakeelya Alkali Member|23282|2|Defined|p75||Early Cambrian|Age: Early Cambrian 522 - 521Ma. of Observatory Hill Formation, Officer Basin. of Brewer et al (1987).||||||
25694|Parakeelya Alkali Member|40945|2|Defined|p6|Late Cambrian|Early Cambrian|Age poorly constrained between Early and Late Cambrian.||||||
25694|Parakeelya Alkali Member|42095|5|Briefly described|Fig.3 P31|||||||||
25694|Parakeelya Alkali Member|42816|6|Mentioned|p14|||of Observatory Hill Formation||||||
25694|Parakeelya Alkali Member|43650|6|Mentioned|Fig.2,p444|||||||||
25694|Parakeelya Alkali Member|43743|6|Mentioned|Fig.2,p33||Early Cambrian|||||||
25694|Parakeelya Alkali Member|44133|5|Briefly described|p37|Middle Paleozoic|Early Paleozoic|Of the Observatory Hill Formation. ||||||07-NOV-08
25694|Parakeelya Alkali Member|62570|5|Briefly described|p580 Figs. 2 and 3|Middle Cambrian|Middle Cambrian|Of Observatory Hill Formation (Marla Group). Geological Province: Officer Basin. Abundant pseudomorphs of the evaporite minerals, trona and shortite, indicate alkalinity and high evaporation rates; dessication cracks and sinter crusts are common.||||||10-AUG-07
25694|Parakeelya Alkali Member|65313|5|Briefly described|p578 Fig. 6|Cambrian|Cambrian|Officer Basin.||Of Observatory Hill Formation.||Underlies Moyles Creek Chert Member, overlies Wallatinna Member.||26-MAR-12
25694|Parakeelya Alkali Member|72478|6|Mentioned|Fig. 7 p70||| Shown as Parakeelya Alkaki Member p8, Parkeelya Alkali Member p69.||||||
25694|Parakeelya Alkali Member|73099|5|Briefly described|Map legend.|Middle Cambrian|Early Cambrian|Officer Basin.||Observatory Hill Formation.||Overlies Cadney Park Member.|Laminated to thin-bedded claystone, siltstone to very fine sandstone, limestone, dolostone and chert; pseudomorphs after evaporitic minerals.|
31519|Pata Formation|23179|6|Mentioned|Fig.2||Middle Miocene|Murray Supergroup||||||
31519|Pata Formation|23226|2|Defined|p901||Balcombian|Was Pata Limestone. Age: Balcombian through presence of foraminfers. Of Murray Supergroup.||||||
31519|Pata Formation|24558|4|Described|p655 Fig. 3||Middle Miocene|Low energy carbonate ramp sediments. Conformably overlies Bryant Creek Formation.||||||
31519|Pata Formation|60785|5|Briefly described|p184 Fig.1, p196.  |Serravallian|Serravallian|South Australia. Balcombian (Middle Miocene) (Lukasik and James, 1998). Has yielded fossil cetacean elements.|||||Yellow-orange fine calcarenite with muddy bands.|
31519|Pata Formation|63460|5|Briefly described|p839 Fig. 2b|Middle Miocene|Middle Miocene|Geological province: Murray Basin. Limestone-rich unit.||||||
31519|Pata Formation|64237|5|Briefly described|p18, p19|Middle Miocene|Middle Miocene|Superseded Pata Limestone of Lawrence (1961). Included as a constituent of the Murray Supergroup of Lukasik and James (1998) and is retained in current Murray Group stratigraphy as a constituent of the group.||||||15-JUL-08
31519|Pata Formation|68716|6|Mentioned|p39 Fig.3, p42 Fig.4, p44, p45 Fig.9|||A semi-confined aquifer. The uppermost aquifer of the regionally confined Murray Group limestone. Source of some saline groundwater discharges to the Murray River.||||Overlain by the Bookpurnong Formation. Underlain by the Winnambool Formation.||07-APR-17
31519|Pata Formation|69372|6|Mentioned|p34 fig. 12|Miocene|Oligocene|||||||
31519|Pata Formation|72445|6|Mentioned|App.6 p2 Fig.1.|Middle Miocene|Middle Miocene|Of Gallagher and Gourlay (2007). See also Pata Limestone App.7.||Shown as part of Murray Supergroup.||Overlies Cadell Formation.|Includes limestone.|
30339|Patsy Hill Member|60418|5|Briefly described|p134 Fig.1|Neoproterozoic|Neoproterozoic|Of Bonney Sandstone.||||||
30339|Patsy Hill Member|60959|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Of the Bonney Sandstone. Limestone-sandstone parasequences.||||||
30339|Patsy Hill Member|61732|5|Briefly described|p28 Fig. 13|Marinoan|Marinoan|Of the Bonney Sandstone. Geological Province: Adelaide Rift Complex.||||||07-FEB-11
30339|Patsy Hill Member|62784|5|Briefly described|p8 Fig.1|Neoproterozoic|Neoproterozoic|Basal member of Bonney Sandstone.||||||
30339|Patsy Hill Member|63569|6|Mentioned|p118 Fig. 2|Neoproterozoic|Neoproterozoic|||Unit in Bonney Sandstone.||||
30339|Patsy Hill Member|64455|5|Briefly described|p138 Fig. 1|Early Cambrian|Ediacaran|Of Pound Subgroup. Light coloured sandstone, dark oolitic carbonate.||||||
30339|Patsy Hill Member|65925|5|Briefly described|Appendix 2.||||||||Limestone, algal-laminated, grey, also wavy/swaley cross-stratified limestone, grading up to thick-bedded calcarenite then to micaceous sandstone. Generally two limestone-sandstone parasequences.|
30339|Patsy Hill Member|68271|5|Briefly described|p695-696|||Adelaide Rift Complex.||Unit of Bonney Sandstone.||||
30339|Patsy Hill Member|70790|5|Briefly described|p259|Ediacaran|Ediacaran|Previously of the Wonoka Formation; reassigned to the Bonney Sandstone by Reid and Preiss (1999).|||||Carbonates.|
30339|Patsy Hill Member|72489|6|Mentioned|p4|Neoproterozoic|Neoproterozoic|Adelaide Rift Complex. Similarities in stromatolite form have been used to correlate this with the Julie Formation.||Bonney Sandstone||Correlated with Julie Formation.||
30339|Patsy Hill Member|73222|4|Described|p6-8, p11-12, p14, p16-21, p23-25|Ediacaran|Ediacaran|Adelaide Rift Complex. Includes informal lower and upper dolomite beds and lower and upper sandstone beds (lower dolomite beds = lithofacies 5) [Described in moderate detail building on previous work but formal names are not given; see article for more detail]. Deposited in a tidally dominated tidal inlet setting. [Article includes O and C stable isotope investigation]. Forms inclusions in the Patawrta Diapir (and in adjacent suprasalt and subsalt minibasins), which suggests active halokinesis during the Ediacaran.||Bonney Sandstone, Pound Subgroup, Wilpena Group, Heysen Supergroup||||
79869|Patterton Member|64801|5|Briefly described|p111-112, p119|Cryogenian|Cryogenian|New, informal name. Unconformity-bound genetic increment of strata [?]. Sediments derived from nearby exposed diapirs. In part equivalent to, or replacing the Wundowie Member of the Enorama Shale?||Enorama Shale.|||Shallow-water stromatolitic, ooid, intraclast and lithoclast limestones, overlain by deeper-water green siltstones which shallow up to stromatolitic limestone again.|21-JUN-17
79869|Patterton Member|72473|6|Mentioned|p4|||||||||
68682|Paxton Granite|60704|2|Defined|p686 Fig.1, p699 App.1|Paleoproterozoic|Paleoproterozoic|Unconformably overlain by the Tarcoola Formation. Intruded by dykes of the Lady Jane Diorite. Age: ca. 1720Ma. Probably of the Mulgathing Complex. Possibly equivalent to the Moody Suite. Monzogranite with finer grained syenogranite, minor quartz monzonite||||||07-NOV-08
68682|Paxton Granite|63224|5|Briefly described|p10|Paleoproterozoic|Paleoproterozoic|Age: 1715Ma. Geological Province: Gawler Craton.||||||07-NOV-08
68682|Paxton Granite|63276|5|Briefly described|p3 Fig. 2, p14 Fig. 3|Paleoproterozoic|Paleoproterozoic|Unconformably overlain by Tarcoola Formation. Age:~ 1715Ma. Predominantly homogeneous coarse-grained hornblende-biotite-titanite monzogranite.||||||07-NOV-08
68682|Paxton Granite|64130|6|Mentioned|p1382, p1837 |||Tarcoola area, central Gawler Craton.|c.1715 Ma (Budd and Fraser, 2004).|||||
68682|Paxton Granite|64137|4|Described|p1541-1562        |Statherian|Statherian|Hosts Tarcoola goldfield. SHRIMP U-Pb zircon age for the quartz monzonite; also 1722.3 +/- 3.9 Ma for the monzogranite, and 1715.1 +/- 3.2 Ma for the syenogranite. Alteration detailed. Nd and Pb isotope data. Samples analysed are near contact with Euro Limestone.|1718.6 +/- 2.9 Ma (Budd, 2006).|||Intruded by dykes of Lady Jane Diorite. Is overlain nonconformably by Tarcoola Formation.|Consists of a homogeneous coarse-grained monzogranite main phase, with lesser finer grained syenogranite and very minor quartz monzonite.|
68682|Paxton Granite|65376|6|Mentioned|p121, pp215-217.||||c.1720 Ma.|||||
68682|Paxton Granite|66302|6|Mentioned|p23|Statherian|Statherian|Ages are SHRIMP U-Pb from Budd (2006).|1722 +/- 4 Ma to 1715 +/- 3 Ma|Tunkillia Suite||||
68682|Paxton Granite|67058|5|Briefly described|p479, p494.|Paleoproterozoic|Paleoproterozoic||1722 +/- 4 to 1715 +/- 3 Ma (Budd & Skirrow 2007).|||Is overlain by Tarcoola Formation.|Monzogranite, syenogranite, quartz monzonite.|
68682|Paxton Granite|67536|6|Mentioned|Map Legend|Statherian|Statherian|Gawler Craton. Of Kimban Orogeny.|ca. 1715 Ma||||Granite.|
68682|Paxton Granite|67980|6|Mentioned|p550|Statherian|Statherian|Budd and Skirrow (2007). Gawler Craton. Associated with Kimban Orogeny (c.1730-1690 Ma).||||||
68682|Paxton Granite|71318|5|Briefly described|p26|Paleoproterozoic|Paleoproterozoic|Geological province: Gawler Craton. Similar in age to granites attributed to the Paxton Suite (U-Pb zircon age 1708+\-13 Ma; Sample GSSA 2017964; this report).||||||
68682|Paxton Granite|71862|4|Described|p7, p11, p13-p14, p23|Statherian|Statherian|Outcrops in the Tarcoola Goldfields of the central Gawler Craton. Intersected in drillholes GP078D GP004D and GP028RD. The syenogranite was dated at 1715 +/- 3 Ma and the quartz monzonite at 1718 +/- 3 Ma (Budd, 2006). See also p33-p34, p42, p59, p62.|1722 +/- 4 Ma (magmatic cryst., Budd, 2006)|Pinbong Suite||Unconformably overlain by the Tarcoola Formation. Intruded by the Lady Jane Diorite.|Monzogranite, syenogranite and quartz monzonite.|19-APR-23
68682|Paxton Granite|73235|6|Mentioned|p61|||Hosts gold mineralisation in the Tarcoola mineral field of the Kararan (Gawler Range Volcanics) gold mineral system.||||||
24453|Pedirka Formation|40910|5|Briefly described|p19|||||||||
24453|Pedirka Formation|40911|6|Mentioned|Map legend|early Pleistocene|Miocene|?Miocene-Early Pleistocene||||||
24453|Pedirka Formation|40925|6|Mentioned|Map legend|Cenozoic|Cenozoic|||||||19-NOV-08
24453|Pedirka Formation|40926|3|Fully described|p28|||||||||
24453|Pedirka Formation|41257|6|Mentioned|p4|||||||||
24453|Pedirka Formation|65489|6|Mentioned|p160|||Eromanga Basin. Possible source of oil in Poolowanna Trough.||||||
28234|Peebinga Soil|39349|6|Mentioned|Map legend|Holocene|Holocene|||||||
28234|Peebinga Soil|42717|5|Briefly described|map legend|Holocene||||||||
28234|Peebinga Soil|43073|5|Briefly described|p18|||||||||
24619|Peera Peera Formation|13497|5|Briefly described|p65, p114|||Simpson Basin. Up to 190m thick.||||Equivalent to the Cuddapan Formation.||
24619|Peera Peera Formation|22839|6|Mentioned|P33|||Lateral equivalent of the Cuddapan Formation||||||
24619|Peera Peera Formation|22857|5|Briefly described|p310|Late Triassic|Late Triassic|Geological Province: Eromanga Basin.||||||
24619|Peera Peera Formation|22865|6|Mentioned|p310||Late Triassic|||||||
24619|Peera Peera Formation|22883|5|Briefly described|P31, Fig2||Late Triassic|Correlated to the Cuddapan Formation, underlying unit is Walkandi Formation.||||||16-SEP-08
24619|Peera Peera Formation|24204|5|Briefly described|p262, 263 Fig.4|Late Triassic|Late Triassic|Shale, coal, sandstone. Overlies Walkandi Formation (unconformable). Geological Province: Simpson Basin.||||||
24619|Peera Peera Formation|36922|6|Mentioned|Fig.3|||Note with Fig.4 states name should be P.P.beds. Misspelling of Peera Perra?||||||
24619|Peera Peera Formation|36941|6|Mentioned|Table 1|||||||||
24619|Peera Peera Formation|37287|6|Mentioned|p36|||||||||
24619|Peera Peera Formation|37776|6|Mentioned|Fig.2|||||||||
24619|Peera Peera Formation|38108|6|Mentioned|Table 1|||Misspelling of Peera Perra?||||||
24619|Peera Peera Formation|41063|2|Defined|p45|Late Triassic|Late Triassic|||||||
24619|Peera Peera Formation|41099|6|Mentioned|Fig.9|||||||||
24619|Peera Peera Formation|41176|6|Mentioned|p206|||||||||
24619|Peera Peera Formation|41183|6|Mentioned|p310|||||||||
24619|Peera Peera Formation|42008|5|Briefly described|p265,266, 267, 268, 275|Late Triassic|Late Triassic|Simpson Desert Basin. Correlated with Cuddapan Formation. Also shown as Peera Perra Formation on p266.||||||09-APR-15
24619|Peera Peera Formation|42062|5|Briefly described|p27|||||||||
24619|Peera Peera Formation|42463|6|Mentioned|Fig.4 P171|||||||||
24619|Peera Peera Formation|42746|4|Described|p6, Fig.2 p4|||||||||
24619|Peera Peera Formation|43052|5|Briefly described|Table 2.1|||||||||
24619|Peera Peera Formation|44133|5|Briefly described|p94|Late Triassic|Late Triassic|Conformably overlies: Walkandi Formation. Maximum Thickness: 190m. ||||||
24619|Peera Peera Formation|62376|5|Briefly described|p84|Late Triassic|Middle Triassic|Geological Province: Pedirka Basin.||||||09-FEB-10
24619|Peera Peera Formation|63979|6|Mentioned|p31|||Geological province: Simpson Basin. Correlate of Cuddapan Formation.||||||07-FEB-11
24619|Peera Peera Formation|64778|6|Mentioned|p13, 28|Triassic|Triassic|Simpson Desert Basin. Potential hydrocarbon source.||||||
24619|Peera Peera Formation|65238|5|Briefly described|p7 Fig. 8, p9|Late Triassic|Middle Triassic|Unconformably overlies Walkandi Formation. Max. thickness: 200m. Geological province: Simpson Desert Basin. Lacustrine, low energy, meandering deposits comprising thick, broadly upward-fining succession. Very detailed lithology included. See also p10.||||||
24619|Peera Peera Formation|65489|5|Briefly described|p53, p55-63, p137, p149-151|Late Triassic|Middle Triassic|Simpson Basin. 190m thick. Hydrocarbon source rock; hosts oil show and gas indication. Poor quality reservoirs; intrafomational siltstone and shale form seals.||||Conformably overlies Walkandi Formation. Correlated with Cuddapan Formation (Cooper Basin). Probably correlates with Tinchoo Formation.|Basal grey shale and siltstone with minor thin sandstone and coal, a fining upward sandy middle unit, and black highly carbonaceous silty shale at the top.|
24619|Peera Peera Formation|69454|5|Briefly described|p38:3-4, 8-13, 14 Fig.38.9|Rhaetian|Carnian|Pedirka Basin (subsurface only). 190m thick in Walkandi-1. Meandering fluvial, lacustrine/paludal deposits. May be equivalent to uppermost part of the Tinchoo Formation. Hosts minor coal resources with fair to good mixed oil-gas source potential. Sandstones have fair to good reservoir potential, with intra-formational shale seals.||||Overlies Purni Formation unconformably, and Walkandi Formation disconformably or unconformably. Is overlain unconformably by Poolowanna Formation. Correlated with Cuddapan Formation (Eromanga Basin).|Shale, siltstone, minor coal and sandstone at base, overlain by cyclical upward-fining sandstone, capped by highly carbonaceous shale with occasional thin sandstone beds.|12-JUL-16
24619|Peera Peera Formation|69457|6|Mentioned|p41:5 Fig.41.4; 41:16|Triassic|Triassic|Fair to good source rocks.||||||12-JUL-16
24619|Peera Peera Formation|69673|5|Briefly described|p152, 159, 160, 161, 149|Triassic|Triassic|190m thick. Source rock potential.||||Unconformably overlies Purni Formation, unconformably overlain by Poolowanna Formation|Shale, siltstone, minor sandstone and coal. Black silty and highly carbonaceous shale with occasional thin sandstone interbeds.|21-SEP-17
24619|Peera Peera Formation|69946|4|Described|p8-9, p36, p51-52|Late Triassic|Late Triassic|Defined by Moore (1986); previously Peera Peera beds of Wiltshire (1978). Type section is the interval 2593 - 2768m in Poolowanna 1. Up to 190m thick. Simpson Basin.||||Conformably overlies Walkandi Formation. Correlated with Cuddapan Formation.|Lowermost (of three) units is siltstone and shale with minor thin sandstone and rare coal; then upward-fining sandstone cycles; topped by black carbonaceous shale, coal and thin sandstone interbeds.|
24619|Peera Peera Formation|69948|6|Mentioned|Fig.4.18|||Eromanga Basin.||||Overlies Walkandi Formation conformably and Purni Formation unconformably. Is overlain unconformably by Poolowanna Formation.||
24619|Peera Peera Formation|71321|6|Mentioned|p15|||Of Simpson Basin.||||Overlies the Walkandi Formation. Overlain by the Poolowanna Formation.||24-OCT-19
24619|Peera Peera Formation|71342|4|Described|Ch4 p25, Ch5 p8-p9|Triassic|Triassic|Simpson Basin. Originally the informal Peera Peera beds of Wiltshire (1978) before being defined by Moore (1986). A type section in Poolowanna 1 is mentioned. This unit was subdivided into three facies by Moore in 1986. A maximum thickness of 190m is recorded in Walkandi 1. Deposited in a high-sinuosity fluvial environment. See also Ch5 p30, Ch5 p36, Ch5 p51-p52, Ch9 p18, Ch11 p6, Ch12 p2-p3, Ch12 tbl 12.1, Ch12 p6, Ch12 p10-p14, Ch14 p4-p7.||||Conformably overlies the Walkandi Formation. Overlain by the Poolowanna Formation.|Siltstone and shale, minor thin sandstone and rare coal. Black carbonaceous shale, coal and thin sandstone interbeds also occurs.|
24619|Peera Peera Formation|72476|6|Mentioned|p36 Fig.9, p37|Triassic|Triassic|Simpson Basin. Time-temperature thermal history diagram. Only 200m thickness preserved.||||||
24619|Peera Peera Formation|73281|6|Mentioned|p1, Appendix (DIP)|Triassic|Triassic|Pedirka Basin. Petroleum source rocks. See DIP034_Petroleumdata.xlsx and DIP034_Welldata.xlsx.||||||
28194|Pember Mudstone Member|22587|6|Mentioned|p79 Fig.7|Early Eocene||||||||
28194|Pember Mudstone Member|22875|5|Briefly described|p26 Table1|||||||||
28194|Pember Mudstone Member|24551|5|Briefly described|p292 Fig. 10.3|||||||||
28194|Pember Mudstone Member|30576|5|Briefly described|Table 2|||||||||
28194|Pember Mudstone Member|30578|6|Mentioned|Table 1|||See also Table 2.||||||
28194|Pember Mudstone Member|30580|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
28194|Pember Mudstone Member|30675|5|Briefly described|p253|||Lithology and radioactivity.||||||27-SEP-07
28194|Pember Mudstone Member|30932|6|Mentioned|Map legend|Eocene|Paleocene|Paleocene - Eocene||||||
28194|Pember Mudstone Member|31036|1|Redefined|p209|Tertiary|Tertiary|See also Table 9-1. Unit of Dilwyn Fm.||||||
28194|Pember Mudstone Member|31372|4|Described|p14|||See also p2, p9.||||||24-JAN-08
28194|Pember Mudstone Member|31424|4|Described|p16|||See also p7. Described from a core.||||||24-JAN-08
28194|Pember Mudstone Member|31922|6|Mentioned|Fig.2|||||||||
28194|Pember Mudstone Member|32852|6|Mentioned|p10|||||||||
28194|Pember Mudstone Member|33940|6|Mentioned|p415|||||||||
28194|Pember Mudstone Member|34360|6|Mentioned|p11|||||||||
28194|Pember Mudstone Member|34988|6|Mentioned|Table 9.4|||||||||
28194|Pember Mudstone Member|35066|6|Mentioned|p205|||||||||
28194|Pember Mudstone Member|36366|5|Briefly described|p3|||||||||
28194|Pember Mudstone Member|37548|5|Briefly described|p129|||||||||
28194|Pember Mudstone Member|41701|6|Mentioned|Map legend|Eocene||||||||
28194|Pember Mudstone Member|41714|6|Mentioned|p301|||||||||
28194|Pember Mudstone Member|41726|6|Mentioned|p421|||See also p427.||||||27-SEP-07
28194|Pember Mudstone Member|41769|4|Described|p23|||||||||
28194|Pember Mudstone Member|42318|6|Mentioned|Fig.2 P10|||||||||
28194|Pember Mudstone Member|42827|5|Briefly described|p280|||Of the Dilwyn Formation.||||||24-JAN-08
28194|Pember Mudstone Member|48911|6|Mentioned|Chart 1|||||||||
28194|Pember Mudstone Member|60563|5|Briefly described|p45 Fig.1, p47|||Of the Dilwyn Formation. Offshore marine deposits.||||||
28194|Pember Mudstone Member|61182|6|Mentioned|p22|||Of Glenie (1965) - introduced this name when he changed Dilwyn Clay to Dilwyn Formation -- for lower part of the formation. In this study Pember Mudstone stands superseded as separate formation.||||||27-SEP-07
28194|Pember Mudstone Member|62896|5|Briefly described|p90 Tb. 1|Late Paleocene|Late Paleocene|See also Pember Mudstone. Of Dilwyn Formation (Wangerrip Group).||||||07-FEB-11
28194|Pember Mudstone Member|63740|5|Briefly described|p89, p90 Tb. 1|Early Eocene|Late Paleocene|Shown as a unit of Wangerrip Group in Table 1 (p90) where it is overlain by the Dilwyn Formation. See also Pember Mudstone - names used interchangeably in study.||||||07-FEB-11
28194|Pember Mudstone Member|65715|5|Briefly described|p11 Tb.7|Paleogene|Paleogene|Of Dilwyn Formation.||||||
28194|Pember Mudstone Member|66002|5|Briefly described|p10 Tb.7,|Paleogene|Paleogene|Of Dilwyn Formation. Defined by Glenie 1971.||||||23-MAY-13
28194|Pember Mudstone Member|71437|5|Briefly described|Fig. 1 opp 154,  p155, p159|Paleocene|Paleocene|||Of Dilwyn Formation.||Transitional contact with underlying Pebble Point Formation, overlying Dilwyn Formation.|Mudstone.|
81038|Pennas Granite|72090|5|Briefly described|p1, p13, p17, p80, p91, p111-p112, p115|||Gawler Craton. Intersected in drillhole MSDP14. This unit hosts a weak, linear magnetic VTEM and ground EM anomaly.||Of Hiltaba Suite.||Intrudes the Corunna Conglomerate.|Porphyritic texture.|18-JUN-19
27876|Pepuarta Tillite|22510|5|Briefly described|p40,table1|||A 'through-going' diamictite unit of the Yerelina Subgroup (together with the Mount Curtis Tillite).  Age: Marinoan. Nackara Arc.||||||13-OCT-04
27876|Pepuarta Tillite|22772|5|Briefly described|Table13.1|Neoproterozoic III|Neoproterozoic III|||||||
27876|Pepuarta Tillite|22857|5|Briefly described|Tb. 13.1 (insert p70-71)|Marinoan|Marinoan|Of the Yerelina Subgroup (Umberatana Group).||||||
27876|Pepuarta Tillite|23818|5|Briefly described|p34 Fig.8, p64 Fig.22, p72|Adelaidean|Adelaidean|Geological Province: Willyama Block. Of the Yerelina Sub-Group. Max. thickness: 600 ft.||||||18-APR-05
27876|Pepuarta Tillite|24364|6|Mentioned|p29 Fig.3|Neoproterozoic|Neoproterozoic|||||||
27876|Pepuarta Tillite|24400|5|Briefly described|p155 Tb.2|Adelaidean|Adelaidean|||||||
27876|Pepuarta Tillite|29778|6|Mentioned|p167|||||||||
27876|Pepuarta Tillite|29780|5|Briefly described|p41|||||||||
27876|Pepuarta Tillite|29837|4|Described|p61|||||||||
27876|Pepuarta Tillite|30261|6|Mentioned|Table 1|||Marinoan age||||||
27876|Pepuarta Tillite|30798|6|Mentioned|p116|||See also Fig.1||||||
27876|Pepuarta Tillite|30801|6|Mentioned|p5|||Marinoan. Table P5-6||||||
27876|Pepuarta Tillite|30802|6|Mentioned|Table 1|||||||||
27876|Pepuarta Tillite|30807|6|Mentioned|p102|||Suggested map symbol||||||
27876|Pepuarta Tillite|30810|6|Mentioned|Fig.1|||||||||
27876|Pepuarta Tillite|32720|6|Mentioned|p5|||666 + or - 56 my. Correlated Egan Glacials. See also P7||||||
27876|Pepuarta Tillite|32722|6|Mentioned|Fig.3|||Adelaidean. Stromatolite||||||
27876|Pepuarta Tillite|32724|6|Mentioned|Fig.1|||Marinoan. Correlation||||||
27876|Pepuarta Tillite|33474|6|Mentioned|Fig.2|||||||||
27876|Pepuarta Tillite|34291|6|Mentioned|p16|||Marinoan. Equiv. Elatina Fm||||||
27876|Pepuarta Tillite|34535|6|Mentioned|p72|||See Fig.22||||||
27876|Pepuarta Tillite|34536|6|Mentioned|Map legend|Adelaidean|Adelaidean|Marinoan||||||
27876|Pepuarta Tillite|34537|6|Mentioned|Fig.8|||||||||
27876|Pepuarta Tillite|34812|6|Mentioned|p134|||||||||
27876|Pepuarta Tillite|35255|6|Mentioned|p13|||||||||
27876|Pepuarta Tillite|36253|6|Mentioned|Fig.3-2|||||||||
27876|Pepuarta Tillite|36833|6|Mentioned|Fig.1|||||||||
27876|Pepuarta Tillite|37461|6|Mentioned|Table 5.I|||See also P342||||||
27876|Pepuarta Tillite|37932|5|Briefly described|p546|||See also P545.||||||
27876|Pepuarta Tillite|38110|6|Mentioned|p2|||||||||
27876|Pepuarta Tillite|38157|6|Mentioned|Table IV|||||||||
27876|Pepuarta Tillite|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Marinoan||||||
27876|Pepuarta Tillite|40442|6|Mentioned|p10|||||||||
27876|Pepuarta Tillite|41405|3|Fully described|p198|||||||||
27876|Pepuarta Tillite|41500|6|Mentioned|Fig.1|||||||||
27876|Pepuarta Tillite|42098|5|Briefly described|p54|||||||||
27876|Pepuarta Tillite|42109|5|Briefly described|Fig.1 P19|||||||||
27876|Pepuarta Tillite|42222|6|Mentioned|p18|||||||||
27876|Pepuarta Tillite|42239|6|Mentioned|p149|||||||||
27876|Pepuarta Tillite|42542|5|Briefly described|p8|||||||||
27876|Pepuarta Tillite|42720|5|Briefly described|map legend|Marinoan||||||||
27876|Pepuarta Tillite|42813|4|Described|p21|||Of the Yerelina Subgroup.||||||14-MAY-07
27876|Pepuarta Tillite|43052|5|Briefly described|p192,Table 6.1|||Of Yerelina Subgroup.||||||30-SEP-08
27876|Pepuarta Tillite|44659|5|Briefly described|map legend|||Marinoan, lithology.||||||
27876|Pepuarta Tillite|44690|4|Described|map legend|||Geol. Atlas Series. (I/54-5). Unit of Umberatana Group. Marinoan.||||||
27876|Pepuarta Tillite|61238|4|Described|p46 Fig. 2, p47 Fig. 3|Neoproterozoic|Neoproterozoic|Of the Umberatana Group. Siltstone and sandy siltstone, sparse granule to boulder erratics, often calcareous.||||||
27876|Pepuarta Tillite|61732|5|Briefly described|p28 Fig. 13|Marinoan|Marinoan|Of the Yerelina Subgroup (Umberatana Group). Geological Province: Adelaide Rift Complex.||||||07-FEB-11
27876|Pepuarta Tillite|67030|6|Mentioned|p409 Fig. 2|Cryogenian|Cryogenian|||Yerelina Subgroup||Overlies Gumbowie Arkose, underlies Grampus Quartzite.||26-APR-12
27876|Pepuarta Tillite|71237|14|Not recorded|p9, p18|||||||||
27876|Pepuarta Tillite|73093|5|Briefly described|map legend|Neoproterozoic|Neoproterozoic||||||Siltstone and sandy siltstone, sparse granule to boulder erratics, pale grey or greyish green, massive or bedded, often calcareous.|09-DEC-21
23898|Perkana Member|22528|6|Mentioned|p43 Fig2||Late Eocene|||||||
23898|Perkana Member|22541|4|Described|P 24, Fig 1, 7|||||||||
23898|Perkana Member|38621|2|Defined|p4|late Eocene|late Eocene|||||||
23898|Perkana Member|40238|5|Briefly described|p125|||||||||
23898|Perkana Member|40429|6|Mentioned|Fig.2|||||||||
23898|Perkana Member|40453|6|Mentioned|Fig.5|||||||||
23898|Perkana Member|40778|6|Mentioned|p530|||||||||
23898|Perkana Member|40877|5|Briefly described|p49|||||||||
23898|Perkana Member|40969|6|Mentioned|Fig.1|||||||||
23898|Perkana Member|41025|6|Mentioned|Fig.3|||||||||
23898|Perkana Member|41513|6|Mentioned|Fig.4|||||||||
23898|Perkana Member|41520|5|Briefly described|Fig.8|||||||||
23898|Perkana Member|41626|6|Mentioned|p56|||||||||
23898|Perkana Member|42574|6|Mentioned|Fig.2 P242|||||||||
23898|Perkana Member|44133|5|Briefly described|p165 Fig. 10.11, 168|Late Eocene|Late Eocene|Geological Province: Saint Vincent Basin. Overlies: Gull Rock Member. Of the Blanche Point Formation. ||||||
23898|Perkana Member|60538|5|Briefly described|p479 Fig. 18|Oligocene|Eocene|Geological Province: Saint Vincent Basin. Of the Blanche Point Formation. Shown as overlying the Gull Rock Member and overlain by the Tuit Member.||||||18-MAR-13
23898|Perkana Member|64397|5|Briefly described|p233 Fig. 2|Late Eocene|Late Eocene|Spicule-rich opal, carbonate, clay. Geological province: St Vincent Basin.||||||
23898|Perkana Member|65891|5|Briefly described|p222 Fig.7, p228 Fig.11.|Paleogene|Paleogene|Unit in Blanche Point Formation, between Gull Rock (below) and Tuit Members. Spiculite-rich.||||||
23898|Perkana Member|70660|4|Described|p9, p12, p17 fig 9c|Priabonian|Priabonian|Previously the 'soft marls' of earlier literature [the author doesn't reference these earlier works]. See also p18-p19, p25-p26, p33, p46.||Blanche Point Formation||Overlies the Gull Rock Member. Overlain by the Tuit Member.|Soft Spongolitic mudstone, highly siliceous.|
23898|Perkana Member|70722|5|Briefly described|p218|Late Eocene|Late Eocene|Of St. Vincent Basin. Equivalent to Kingscote Limestone Unit K1 of this study.||Unit of Blanche Point Formation.||Overlain by Tuit Member. Underlain by Gull Rock Member.||
23898|Perkana Member|73188|6|Mentioned|p320|Late Eocene|Late Eocene|St Vincent Basin.||Blanche Point Formation||||
28918|Pernatty Grit|31317|5|Briefly described|p162|||||||||
28918|Pernatty Grit|31324|5|Briefly described|p159|||||||||
28918|Pernatty Grit|44538|4|Described|map legend|||(H/53-16). Geol.Atlas Series. Umberatana Group Equivalent. Sturtian.||||||
28918|Pernatty Grit|72247|6|Mentioned|p39-40|Neoproterozoic|Neoproterozoic|Of Adelaide Geosyncline. Obsolete. Nomenclature of Johns 1968, citing the interval between 239-611m in the Woomera Bore as representative of the Pernatty Grit.||||||
29842|Peryhumuck Formation|22884|2|Defined|p40 Fig. 1, p43||Statherian|Of Thackaringa Gp (Willyama Supergp). Overlain by Meningie Well Fm. Correlates with Himalaya Fm (Broken Hill Domain).  Ages: 1785+/-16 Ma and 1775 Ma. Overlain by Meningie Well Fm. Plagioclase-rich metasediment + minor thin ironstone +quartzofeldspathic||||||26-MAR-09
29842|Peryhumuck Formation|61736|5|Briefly described|p666 Fig. 3|Paleoproterozoic|Paleoproterozoic|Of Ethiudna Subgroup (Curnamona Group). Age: 1712+/-2Ma and 1715+/-3Ma. Geological province: Olary Domain.||||||
29842|Peryhumuck Formation|62535|5|Briefly described|p666 Fig.3, p672|Paleoproterozoic|Paleoproterozoic|Olary Domain.|1715 +/- 3 Ma; 1712 +/- 2 Ma.|Ethiudna Subgroup.||||
29842|Peryhumuck Formation|62993|4|Described|p2, p6, p7, p13, p37|Paleoproterozoic|Paleoproterozoic|Olary Domain and Broken Hill Domain?||Ethiudna Subgroup||Overlies Tommie Wattie Formation, George Mine Formation.|Fine grained albitic  and calc-albitic metasilstones containing meta-amphibolite upon which a breccia body is focussed. Epidote rich metasiltstone.|17-DEC-21
29842|Peryhumuck Formation|63102|4|Described|p14,17,20-22,27,30-31,34,37,54,59|Statherian|Statherian|Geological province: Olary Domain, Curnamona Province. Formerly known as Peryhumuck Calcalbitite. Includes Esso's "Upper  Albite" unit (Laing 1996b). Outcrops on the Benagerie Ridge, and thickens under cover to several hundred meters at Waulakoo and Burdens Dam. Uniquely characterised by hydrothermal brecciation. Equivalent to calc-albitites in the Tommie Wattie Formation. Sedimentary structures indicate deposition in relatively shallow sub-aqueous conditions, with evidence of emergence and evaporitic conditions (rhomb-shaped calc-silicate and rare haematite pseudomorphs). Diverse rock composition (ranging from Na-rich to Na- (Ca-Mg)-rich and locally to K-rich, Fe-rich, Mn-rich and B-rich), resulting from clastic quartzofeldspathic sedimentation (in part of felsic igneous provenance) and interaction with evaporative brines, together with chemical sedimentation of evaporites and local hot spring exhalites (Cook and Ashley, 1992; Cook, 1993; Dibben, 1990). Interlayered with volcanic lenses and material of the Abminga Subsuite.|1717 +/- 3 Ma (U-Pb)|Unit of Ethiudna Subgroup.||Underlain by Tommie Wattie Formation. Equivalent to Thackaringa Group, Thorndale Composite Gneiss, Clevedale Migmatite.|Dark grey, well laminated, rather fine-grained, albite - quartz (+\-K-feldspar, biotite, magnetite, calcsilicates) metasediment.|22-OCT-19
29842|Peryhumuck Formation|64741|5|Briefly described|p301 Fig. 4|Paleoproterozoic|Paleoproterozoic|Of Ethiudna Subgroup (Curnamona Group). Geological province: Olary Domain.||||||07-FEB-11
29842|Peryhumuck Formation|64944|4|Described|p27, p28 Fig. 1, p29 Tb. 1|Paleoproterozoic|Paleoproterozoic|Of Ethiudna Subgroup (Curnamona Group). Age: ~1715Ma. Geological province: Olary Domain. Evaporitic unit. Calc-albitite metasiltstone, locally pseudomorphs after carbonate and others.||||||07-FEB-11
29842|Peryhumuck Formation|66302|5|Briefly described|p36 Fig.9, p37, p39|Statherian|Statherian|Olary Domain, Curnamona Province. ||Ethiudna Subgroup||Overlies the Toraminga Formation, Bewooloo Formation and the Cathedral Rock Formation. Overlain by the Whey Whey Formation and the Waukaloo Formation.||
29842|Peryhumuck Formation|67540|6|Mentioned|p31 Tb.2|||||Of the Willyama Supergroup.||Intruded by Lake Charles Diorite.||03-FEB-16
29842|Peryhumuck Formation|69650|5|Briefly described|p6, p42|||||Unit in Willyama Supergroup.||Intruded by Lake Charles Diorite.|Includes laminated albitites.|
29842|Peryhumuck Formation|70339|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|Members not clearly stated, but implied from map symbols used.|||Includes Koolka Ironstone Member. Probably includes Whey Whey Member, Faugh-a-Ballagh Member also.||Metasediment, alkali-feldspar+calc-silicate. Disseminated magnetite or haematite, evaporitic or diagenetic pseudomorphs, shallow-water to emergent sedimentary structures.|
29842|Peryhumuck Formation|70340|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|||Probably of Ethiudna Subgroup.|||Metasediment, alkali-feldspar+calc-silicate. Disseminated magnetite or haematite, evaporitic or diagenetic pseudomorphs, shallow-water to emergent sedimentary structures.|
29842|Peryhumuck Formation|70405|4|Described|p19, p21, p22, p25, p26 plate 5, p36, |Paleoproterozoic|Paleoproterozoic|Protoliths of siltstone to fine grained sandstone with variable feldspar, clay and carbonate. Copper deposit located in psammite and calc-albitite. Includes four facies variations (unnamed and not all present in region). Intruded by Nancatee Granite.|1710 Ma-1715 Ma|Ethiunda Subgroup|Includes Faugh-a-ballagh Member, Koolka Ironstone Member Waukaloo Member, Whey Whey Member|Overlies Tommie Wattie Formation and Toraminga Formation, also overlies Cathedral Rock Formation, Interfingers with Whey Whey Member, underlies Waukaloo Member, Telechie Sulphide Member|Fine-medium grained, thinly bedded, commonly well laminated fine grained psammite; psammopelitic, pelitic, psammitic schists and local chemical sediments. Alkali-feldspathic and calcareous metasediments all intergrading laterally and vertically.|
29842|Peryhumuck Formation|70657|4|Described|p14-15, p22-24, p26-31, p59-60, p65|Statherian|Statherian|Laing (1996); redefined by Conor (2000). Curnamona Province; Olary Domain. No equivalent in Broken Hill Domain. Spectacular hydrothermal brecciation. Varied rock compositions are attributed to shallow sub-aqueous to evaporitic conditions with local hot-spring activity, and metasomatism (described). Ca-Fe alteration mentioned.|<1717 +/- 3 Ma  - ~1710 Ma|Ethiudna Subgroup||Overlies Toraminga, Bewooloo, Cathedral Rock, Mooleugore and (transitionally) Tommie Wattie Formations. Underlies Whey Whey and Waukaloo Formations.|Albitic and calc-albitic metasiltstone to fine-grained metasandstone commonly showing shallow water sedimentary structures and pseudomorphs after evaporitic minerals.|
29842|Peryhumuck Formation|70658|5|Briefly described|p1-2, 4-12, 15, 18-21, 23, 25-29, 32|Paleoproterozoic|Paleoproterozoic|See also p39-40. Olary Domain, Curnamona Province. Hosts large hydrothermal breccia bodies, locally mineralised (eg the Walparuta Cu-Au mine).|~1715 Ma.|Ethiudna Subgroup.|Whey Whey, Faugh-a-Balagh Members.|Gradationally overlies Toraminga Formation. Is overlain by Larry Macs Subgroup. Is intruded by Lady Louise Suite.|Characteristically fine-grained, blue-grey calc-metasiltstone; locally altered to an alkali-feldspar granofels.|
79270|Peter Pan Supersuite|71037|5|Briefly described|p21 Fig.1, p22-23 Fig.2, p24, p25 Fig.4|Paleoproterozoic|Paleoproterozoic||1745-1700 Ma||Includes Moola Suite.|Shown as younger than Wallaroo Group.|Syenite, granite, monzonite, diorite and gabbro, undeformed to weakly foliated.|19-APR-23
79270|Peter Pan Supersuite|71129|5|Briefly described|p14,17-18,40,205|Statherian|Statherian|Geological Province: Cleve-Coulta, Spencer and Olympic domains, Gawler Craton. Bimodal magmatism associated with c. 1740-1690 Ma Kimban Orogeny.|1745-1690 Ma||Includes Moola, Pinbong and Moody suites.||Bimodal magmatic rocks.|13-NOV-19
79270|Peter Pan Supersuite|71131|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic||1745-1700 Ma.||Moola Suite.|||
79270|Peter Pan Supersuite|71317|4|Described|p1, p16, p114, p175|Palaeoproterozoic|Palaeoproterozoic|Nuyts Domain, Gawler Craton. Together with the Tunkillia and Saint Peter Suites forms the basement on the Peltabinna mapsheet.|c. 1745-1700 Ma||Includes the Pinbong Suite.|Overlain by the Gawler Range Volcanics.||
79270|Peter Pan Supersuite|71348|6|Mentioned|p201|Statherian|Statherian|Geological province: Gawler Craton.||||||
79270|Peter Pan Supersuite|71413|6|Mentioned|p32 Fig 2|||Geological province: Gawler Craton. ||||||
79270|Peter Pan Supersuite|71418|6|Mentioned|p21|Paleoproterozoic|Paleoproterozoic|Geological province: Gawler Craton.||||||
79270|Peter Pan Supersuite|71534|5|Briefly described|p296|Statherian|Statherian|Geological province: Gawler Craton. Bimodal magmatism associated with c. 1730-1690 Ma Kimban Orogeny.||||||
79270|Peter Pan Supersuite|71559|6|Mentioned|p15 Fig 1, p16 Fig 2, p19, p22|Statherian|Statherian|Geological province: Gawler Craton.|1745-1700 Ma||Includes Pinbong Suite.|Basement includes Peter Pan Supersuite and Tunkillia Suite||
79270|Peter Pan Supersuite|71560|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Solid Geology part of map sheet.|||Pinbong Suite.|||
79270|Peter Pan Supersuite|71859|5|Briefly described|p2, p4, p6, p11-p12, p18, p35-p36|Statherian|Statherian|Southern Gawler Craton; Cleve, Coulta, Spencer and Olympic domains.|1745-1700 Ma|||Intrudes the Sleaford Complex.||
79270|Peter Pan Supersuite|71862|2|Defined|p1-p2, p4-p5, p11-p12|Statherian|Statherian|Gawler Craton. Named for the Peter Pan Dam, Eyre Peninsula. This supersuite is widely distributed throughout the Gawler Craton, predominantly on the Eyre Peninsula; however, it also outcrops in the eastern Gawler Craton, the Tarcoola area and the Peake and Denison Inliers, Coober Pedy Ridga, Yoolperlinna Inlier and the Fowler Domain. Defined to replace parts of the Lincoln Complex which are synchronous with the Kimban Orogeny. Geochemistry is discussed broadly. Originally thought to span from 1730-1690 Ma (Hoek and Schaefer, 1998) recent dating shows it to predate 1740 and intrusion continued until the end of metamorphism at 1700 Ma. Intruded by the Gawler Range Volcanics. See also p19, p36, p42-p44, p52-p53.|1745-1700 Ma||Includes the Moola Suite, Pinbong Suite and the Moody Suite.|Intrudes the Sleaford Complex, Hutchison Group, Broadview Schist and Moonabie Formation. Locally unconformably overlain by the Corunna Conglomerate and Tarcoola Formation.|Undeformed, weakly foliated, gneissic to migmatitic mafic to felsic alkaline intrusives, including gabbro, gabbroic diorite, monzogabbro, monzodiorite, monzonite, syenite, quartz monzonite, granodiorite and granite.|19-APR-23
79270|Peter Pan Supersuite|72090|4|Described|p10, p14, p60-p62|Statherian|Statherian|Cleve-Coulta Domain, Gawler Craton. Misspelt as the Peter Pan Supersite on p14. Additional lithological descriptions are provided. Can be distinguished from GRV volcanics based on differences in geochemistry. See also p64-p66, p73, p78, p80-p81, p98, p102, p111, p113, p118-p119.|1745-1700 Ma||Includes the Moola Suite.|Unconformably overlain by the Waganny Dacite.|Greyish orange to pink, pegmatitic to schistose, fine to coarse-grained metagranite and minor microgranite; very pale brown, brecciated, medium grained metagranite.|
79270|Peter Pan Supersuite|72242|6|Mentioned|p27|Statherian|Orosirian|Geological province: Coompana Province, Western Gawler Craton.||||||
79270|Peter Pan Supersuite|72463|6|Mentioned|p2|Paleoproterozoic|Paleoproterozoic|||||||
79270|Peter Pan Supersuite|72464|6|Mentioned|p2|Paleoproterozoic|Paleoproterozoic|Gawler Craton.||||||
79270|Peter Pan Supersuite|73092|6|Mentioned|p2, p49|Paleoproterozoic|Paleoproterozoic|||||||
79270|Peter Pan Supersuite|73103|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Intruded during the Kimban Orogeny.|~1750 - 1700 Ma.||||Magmatic rocks, felsic and lesser mafic.|
79270|Peter Pan Supersuite|73104|5|Briefly described|[See comments]|Statherian|Statherian|Geochron represents magmatic crystallisation ages; these corroborate previous age data for 1710-1735 Ma Kimban magmatism in the area. Ages on zircon rims also indicates isotope disturbance coincident with the Delamerian Orogeny. Inferred basement rock of the Mount Double area. Recorded in younger igneous and sedimentary rocks as inherited or detrital igneous zircons. Possible correlative of xenoliths found in the Nummee Granodiorite. p: 1-2, 4-5, 11, 24, 29, 37, ~39-51, 59, 61, 68, 71-72, 75-76.|1723 +/- 5 Ma, 1718 +/- 4 Ma, c. 1735-1710 Ma||Pinbong Suite|Intrudes Sleaford Complex.|Includes fine-coarse grained meta-intermediate igneous units, pegmatite, medium-grained, equigranular, weakly foliated metagranite.|
79270|Peter Pan Supersuite|73110|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Intruded during the Kimban Orogeny.|~1750 - 1700 Ma.||||Magmatic rocks, felsic and lesser mafic. Includes undeformed pegmatite of inferred Kimban age (mapped separately).|
79270|Peter Pan Supersuite|73130|6|Mentioned|[poster] Fig.1|Paleoproterozoic|Paleoproterozoic|||||||28-OCT-22
79270|Peter Pan Supersuite|73165|6|Mentioned|p621|Statherian|Statherian|Gawler Craton. Associated with the ca 1730-1690 Ma Kimban Orogeny.|ca 1745-1700 Ma|||||
79270|Peter Pan Supersuite|73235|6|Mentioned|p53, p59|Statherian|Statherian|Gawler Craton. Deformed felsic intrusives at the Weednanna deposit are assumed to belong to this unit.|1740-1700 Ma|||||
39866|Petermann Nappe Complex|24442|5|Briefly described|p29|||Geological Province: Amadeus Basin.||||||
39866|Petermann Nappe Complex|24497|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
39866|Petermann Nappe Complex|61154|5|Briefly described|p2, p22 Fig. 16|||Name refers to a structural subdomain on the northwestern margin of the Musgrave Block.  See also p33.||||||
39866|Petermann Nappe Complex|69003|5|Briefly described|p67|||Northern Petermann Orogen. Comprises discrete upper crustal shear zones with low-grade synorogenic metamorphism (<640 oC; <650 MPa).||||||
39866|Petermann Nappe Complex|69091|5|Briefly described|p79, p88, p145|||Mapped in the Northern Territory.|590 Ma to 560 Ma|||||
39866|Petermann Nappe Complex|69436|4|Described|p21:3, 17-20|||Western Mulga Park Domain. A 200km wide,  internally duplexed basement-cored wedge, consisting of interleaved basement and basal Amadeus Basin sedimentary rocks, that has been thrust northwards during the Petermann Orogeny. Described in detail.||||||12-JUL-16
39866|Petermann Nappe Complex|73437|6|Mentioned|p153, p157, p160, p162|||Contains rocks of the Musgrave region interleaved with the basal sedimentary sequence of the Aamadeus Basin during the Petermann Orogeny. Lower greenschist facies in northern part. Characterised by structures of foreland fold and thrust belts. Zircon (U-Th)/He cooling ages of 546+/-52 Ma and 531+/-72 Ma from northern end. Apatite fission track ages of 388-271 Ma indicate cooling, exhumation during latest stage of the Alice Springs Orogeny.||||||
24620|Petermorra Volcanics|22631|6|Mentioned|table1, p176|Calymmian|Calymmian|Age: 1550-1560Ma||||||
24620|Petermorra Volcanics|23478|5|Briefly described|p27|Calymmian|Calymmian|Age: 1560+/-2 Ma,||||||12-NOV-14
24620|Petermorra Volcanics|42624|2|Defined|p19|Mesoproterozoic|Mesoproterozoic|Reserved.||||||
24620|Petermorra Volcanics|43052|5|Briefly described|p148|||||||||
24620|Petermorra Volcanics|43053|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Felsic metavolcanics; quartzite, phyllite.||||||26-MAY-05
24620|Petermorra Volcanics|43258|5|Briefly described|Map Legend||Mesoproterozoic|||||||
24620|Petermorra Volcanics|43298|5|Briefly described|Map Legend||Mesoproterozoic|||||||
24620|Petermorra Volcanics|50605|5|Briefly described|p(ii), 10.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Gawler Craton & Curnamona Province. Of the Babbage supersuite. Age: 1560 +/- 3Ma (U-Pb).||||||
24620|Petermorra Volcanics|60953|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Age: 1560Ma. Porphyritic dacite to rhyolite.||||||
24620|Petermorra Volcanics|61108|5|Briefly described|map legend|Mesoproterozoic|Mesoproterozoic|Porphyritic dacite to rhyolite. Age: 1560 Ma.||||||
24620|Petermorra Volcanics|62962|5|Briefly described|p2284 Fig. 2|Mesoproterozoic|Mesoproterozoic|Age: 1560+/-2Ma (Sheard et al., 2003). Geological Province: Mount Painter Province.||||||07-FEB-11
24620|Petermorra Volcanics|64722|5|Briefly described|p15|Proterozoic|Proterozoic|With the Mount Neill Granite, part of a succession of felsic volcanic and intrusive rocks that range in age from 1780-1550 Ma and overlie the Radium Creek Metamorphics. Have a within-plate geochemical signature.||||||
24620|Petermorra Volcanics|66302|6|Mentioned|p39, p50|||Moolawatana Domain, Curnamona Province.||||||
24620|Petermorra Volcanics|67536|6|Mentioned|Map Legend|||Curnamona Province. Mapped with Pepegoona Porphyry as M39.|||||Dacite to rhyolite and volcaniclastic and epiclastic rocks; rhyolitic to rhyodacitic metavolcanic rock|
24620|Petermorra Volcanics|67581|6|Mentioned|p45|||Curnamona Province.||||||
24620|Petermorra Volcanics|67653|6|Mentioned|p4|||Geological province: Curnamona Province. ||||||
24620|Petermorra Volcanics|68068|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Curnamona Province.|1560 +/- 2 Ma (U-Pb zircon).|||Is intruded by White Well Granite and Prospect Hill Granite.|Basal sericitic sandstone; meta-quartz-feldspar porphyry and associated volcaniclastics to epiclastics, strongly deformed, poorly bedded to massive, grey to dark grey with post-emplacement tourmaline clots.|12-NOV-13
24620|Petermorra Volcanics|68126|6|Mentioned|p6|Mesoproterozoic|Mesoproterozoic|Mount Painter Inlier, Curnamona Province.||||||
24620|Petermorra Volcanics|68713|5|Briefly described|p19|Calymmian|Calymmian|Crop out as a series of low E-W trending ridges in the Prospect Hill area, but is limited in its western extension.|ca. 1560 Ma||||Igneous rocks.|
24620|Petermorra Volcanics|69019|4|Described|p20-22, p66.|Calymmian|Calymmian|Curnamona Province. Defined by Sheard et al.(1992); formerly included in Mount Neill Granite Porphyry (Coats et al. 1969).  Mt. Babbage Inlier. Heralds onset of felsic igneous activity. Geochemistry is detailed.|1560 +/- 2 Ma U-Pb zircon (Sheard et al. 1992).||||Meta-quartz-feldspar porphyry (rhyolite to dacite), and associated meta-volcaniclastics to meta-epiclastics; poorly bedded or massive; strongly deformed.|
24620|Petermorra Volcanics|69023|4|Described|p23, p27-33, p46-50, p53, p77, p189,p202|Mesoproterozoic|Mesoproterozoic|Originally included in Mount Neill Granite Porphyry (Coats and Blissett, 1971); excluded from redefined Mount Neill Granite (Sheard et al., 1992; Teale, 1993). Geochemistry detailed.|1560 +/- 3 Ma U-Pb zircon (Sheard et al., 1992).|||Is intruded by White Well and Prospect Hill Granites. Is overlain unconformably by Paralana Quartzite.|Volcanic rhyolitic porphyries with subordinate volcanic rhyodacite to dacite; volcaniclastic, epiclastic lithic sandstones; basal sericitic sandstone. Abundant ovoid K-feldspar phenocrysts typical.|
24620|Petermorra Volcanics|69562|5|Briefly described|p670 Tb.5|||Magmatic crystalisation age.|1560 +/- 3 Ma (Teale and Flint, 1993).||||Deformed felsic extrusive, volcaniclastics, epiclastic sandstone.|06-APR-22
24620|Petermorra Volcanics|69654|6|Mentioned|p3|||Curnamona Province.||||||
24620|Petermorra Volcanics|70384|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|A basal un-named sericitic sandstone member with no observable bedding, is separately mapped. This sub-unit also contains tourmaline clots.|1560 +/- 3 Ma (TIMS U-Pb zircon).|||Is intruded by White Well Granite.|Meta-quartz-feldspar porphyry (rhyolite to dacite) and associated volcaniclastics to epiclastics; the volcanics are strongly deformed, poorly bedded to massive, grey to dark grey and contain post-emplacement tourmaline clots (hydrothermal).|
24620|Petermorra Volcanics|72454|6|Mentioned|p2 Fig.2|Mesoproterozoic|Mesoproterozoic|Part of Mount Painter Inlier.  Shown only on p2 Fig.2.||||||
24620|Petermorra Volcanics|72456|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Marree 1:250k map sheet. Also Solid Geology Interpretation legend.|1560 +/- 3 Ma (U-Pb zircon)||||Deformed, felsic porphyritic extrusives volcaniclastics and epiclastic sandstone.|09-SEP-22
24620|Petermorra Volcanics|72461|6|Mentioned|p6||||1560 +/- 2 Ma|||||
24620|Petermorra Volcanics|75063|6|Mentioned|p93|Mesoproterozoic|Mesoproterozoic|Curnamona Province.|1560-1550 Ma.||||Felsic igneous rocks.|
79271|Pinbong Suite|71037|6|Mentioned|p21 Fig.1|Paleoproterozoic|Paleoproterozoic|Shown only on 'Outcropping geology and mineral deposits of northern Eyre Peninsula' map p21 Fig.1.||||Shown as younger than Moola Suite and older than Tunkillia Suite.||
79271|Pinbong Suite|71129|5|Briefly described|p40|Statherian|Statherian|Geological Province: Gawler Craton. |1740-1700 Ma|Unit of Peter Pan Supersuite.||||
79271|Pinbong Suite|71317|4|Described|p19|Palaeoproterozoic|Palaeoproterozoic|Gawler Craton. Contains basement rocks previously assigned to the Lincoln Complex. |c. 1735 Ma|Peter Pan Supersuite|||A leucocratic, weakly foliated, aphibole bearing microgranite intruded by a massive metadolerite dyke.|
79271|Pinbong Suite|71418|6|Mentioned|p21|Paleoproterozoic|Paleoproterozoic|Geological province: Gawler Craton.||||||
79271|Pinbong Suite|71559|4|Described|p15 Fig 1, p19, p22|Paleoproterozoic|Paleoproterozoic|Geological province: Gawler Craton.Crystallisation age by SHRIMP U-Pb dating.|1735-1700 Ma|Unit of Peter Pan Supersuite.|||Grey, fine- to medium-grained, equigranular to porphyritic biotite granite; weakly-deformed to migmatic; fine- to mediumg-grained,equigranular dolerite and gabbro in the sub-surface.|19-JUN-19
79271|Pinbong Suite|71560|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Solid Geology part of map sheet.|c.1735-1700 Ma (U-Pb SHRIMP).|Peter Pan Supersuite.|||Grey, fine- to medium-grained, equigranular to porphyritic biotite granite; weakly deformed to migmatitic; fine- to medium-grained, equigranular dolerite and gabbro in the subsurface.|16-APR-18
79271|Pinbong Suite|71862|2|Defined|p1, p3, p6-p8, p11-p12, p15-p16, p19|Statherian|Statherian|Gawler Craton. Named after Little Pinbong Rockhole on northern Eyre Peninsula, 544042mE, 6366761mN, GDA94, Zone 53. The most widespread suite in the Peter Pan Supersuite, occuring on central and southern Eyre Peninsula, the Olympic Domain, Coober Pedy Ridge and in the central Gawler Craton. Geochemistry is discussed broadly. Comparable geochemistry with the Moola Suite suggests a genetic relationship. Includes unnamed granite outcrops. Intersected in drillholes DDH BUDD 23, DDH BUDD 28, DDH BUDD 168, WDDH01 and DDH RD 160.  See also p21-p22, p30, p33-p34, p36, p42-p45, p52, p58-p62.|1735-1700 Ma|Peter Pan Supersuite|Includes the Middle Camp Granite, Carappee Granite, Colona Gabbro and the Paxton Granite.||Equigranular, foliated, gneissic and migmatitic quartz-feldspar-biotite granite and K-feldspar megacrystic granite, feldspar-quartz-muscovite granite, monzogranite, syenogranite, gabbro and dolerite.|
79271|Pinbong Suite|72463|6|Mentioned|p2|Paleoproterozoic|Paleoproterozoic|||||||
79271|Pinbong Suite|72464|6|Mentioned|p2|Paleoproterozoic|Paleoproterozoic|Gawler Craton.||||||
79271|Pinbong Suite|72484|6|Mentioned|p2|||Associated with the transpressive, amphibolite- to granulite-facies metamorphism of the Kimban Orogeny.|1735-1700 Ma.|||||
79271|Pinbong Suite|73103|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic||~1735-1700 Ma (crystallisation).||||Granite to quartz monzonite, typically grey, plagioclase-rich, mica-bearing, weakly deformed to migmatitic; lesser gabbro, dolerite.|
79271|Pinbong Suite|73104|6|Mentioned|p51|||Mount Double map sheet.||Peter Pan Supersuite|||Metagranites and granitic gneisses.|
78806|Pinding Granite|64137|6|Mentioned|p1553 Fig.8 |||Of Stewart and Foden (2001). Neodymium isotope data.||||||
26843|Pindyin Sandstone|22746|5|Briefly described|Fig.3 p515|Cryogenian|Cryogenian|||||||
26843|Pindyin Sandstone|22922|5|Briefly described|32|||||||||
26843|Pindyin Sandstone|23282|2|Defined|p50||Neoproterozoic|Age: Precambrian, Neoproterozoic, Willouran to Tourensian Epochs.||||||
26843|Pindyin Sandstone|23286|6|Mentioned|p89||Neoproterozoic|equivalent to Heavitree Quartzite.||||||
26843|Pindyin Sandstone|23288|4|Described|Fig.6 p125||Neoproterozoic|see also Fig.5, 18. of Early Neoproterozoic Torrensian succession. Was Pindyin beds (Major 1973). Full explanation of acritarch assemblage. of Officer Basin.||||||
26843|Pindyin Sandstone|23479|5|Briefly described|p26|||Geological Province: Gawler Craton.||||||
26843|Pindyin Sandstone|23524|5|Briefly described|p221 Fig. 3|Neoproterozoic|Neoproterozoic|||||||
26843|Pindyin Sandstone|23818|4|Described|p55|||Geological Province: Officer Basin. Equivalent of the Upper Callanna Beds. Overlying unit: Wright Hill Formation.||||||
26843|Pindyin Sandstone|24112|5|Briefly described|p254 Fig.2|Neoproterozoic|Neoproterozoic|Of the Callanna Group. Geological Province: Officer Basin||||||
26843|Pindyin Sandstone|30807|6|Mentioned|p103|||Suggested map symbol||||||
26843|Pindyin Sandstone|31914|6|Mentioned|p95|||||||||
26843|Pindyin Sandstone|31965|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
26843|Pindyin Sandstone|31967|6|Mentioned|p.3|||||||||
26843|Pindyin Sandstone|33468|6|Mentioned|p212|||||||||
26843|Pindyin Sandstone|33478|6|Mentioned|p454|||||||||
26843|Pindyin Sandstone|34535|5|Briefly described|p55|||||||||
26843|Pindyin Sandstone|35308|6|Mentioned|p454|||||||||
26843|Pindyin Sandstone|43657|6|Mentioned|p3||Neoproterozoic|||||||
26843|Pindyin Sandstone|43690|6|Mentioned|p155||Neoproterozoic|||||||
26843|Pindyin Sandstone|43743|6|Mentioned|Fig.2,p33||Neoproterozoic|||||||
26843|Pindyin Sandstone|44109|5|Briefly described|p17, p22 Fig. 19|Willouran|Willouran|Together with Alinya Formation, forms the basal units of the Officer Basin. Geological Province: central Officer Basin.||||||
26843|Pindyin Sandstone|60953|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Fluvial to shallow marine sandstone, minor shale. Age and correlation uncertain.||||||
26843|Pindyin Sandstone|61108|5|Briefly described|map legend|Adelaidean|Adelaidean|Fluvial to shallow marine sandstone and minor shale. Age and correlation uncertain.||||||
26843|Pindyin Sandstone|62453|4|Described|p5 Fig. 3, 14, 17, 18|Cryogenian|Cryogenian|Geological Province: Officer Basin. Possibly synonym with Townsend Quartzite. Previously Pindyin Beds.||||||14-OCT-08
26843|Pindyin Sandstone|63397|6|Mentioned|5|Neoproterozoic|Neoproterozoic|||||||
26843|Pindyin Sandstone|63811|6|Mentioned|p506, 523|Cryogenian|Cryogenian|Present in the Giles 1 Drillhole, Officer Basin.||||||28-MAR-12
26843|Pindyin Sandstone|64103|6|Mentioned|p400 Fig. 3|Cryogenian|Cryogenian|Geological Province: Officer Basin.||||||07-FEB-11
26843|Pindyin Sandstone|64794|6|Mentioned|p238 fig 2|Cryogenian|Cryogenian|||||||
26843|Pindyin Sandstone|64970|6|Mentioned|p719 Fig. 2|Neproterozoic|Neoproterozoic|Geological Province: Officer Basin.||||||27-MAY-09
26843|Pindyin Sandstone|65376|6|Mentioned|p247 Fig.6.57.|Neoproterozoic|Neoproterozoic|||||||
26843|Pindyin Sandstone|67120|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic||||||Basal conglomerate, coarse-grained and gritty sandstone, cross-bedded, overlain by shale with chert beds, limestone and dolomite.|
26843|Pindyin Sandstone|67536|6|Mentioned|Map Legend|||Mapped with Alinya Formation as N3.|||||Fluvial to shallow marine sandstone, minor shale; tidal to sabkha siltstone, shale, sandstone with anhydrite.|
26843|Pindyin Sandstone|67912|6|Mentioned|p26|Cryogenian|Cryogenian|Possible equivalent of the Ediacaran-aged Younghusband Conglomerate.||||||
26843|Pindyin Sandstone|67921|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Shown only in section as Callanna/Burra Group equivalents, including Pindyin Sandstone.||||||
26843|Pindyin Sandstone|68270|5|Briefly described|p683|Tonian|Tonian|Eastern Officer Basin.||||Overlain by Alinya Formation. Underlain by basement.||
26843|Pindyin Sandstone|69203|5|Briefly described|p11-12, p57, p59|Neoproterozoic|Neoproterozoic|Officer Basin. Overlies the basement of the Yoolperlunna Inlier. Is interpreted to underlie Bulldog Shale in GOMA DH1.||Callana Group.|||Extremely hard massive quartzite.|
26843|Pindyin Sandstone|69648|4|Described|p17-18, p34, map legend|Neoproterozoic|Neoproterozoic|Age: Willouran. Probable equivalents of this unit have been interpreted from drillhole logs. No outcrop on OOLDEA. In drillhole (GOD/SAN YL1) the maximum observed thickness is 58 m. In central Officer Basin, basal bed of lowstand conglomerate thins to south, followed by 190 m thick sandstone (herringbone cross-bedding, probably a marine transgression). ||||Conformably overlain by Alinya Formation.|White to dark red, very fine to coarse-grained quartz sandstone, locally pyritic or hematitic with interbeds of dolomitic mudstone and calcareous sandstone; basal conglomerate.|
26843|Pindyin Sandstone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone|
26843|Pindyin Sandstone|71268|5|Briefly described|1m_geologyp12_lut.csv|||||Unit of Callanna Group.|||Basal conglomerate, coarse-grained and gritty sandstone, cross-bedded, overlain by shale with chert beds limestone and dolomite.|
26843|Pindyin Sandstone|72478|5|Briefly described|p8, p24-26, p28, 33|Neoproterozoic|Neoproterozoic|Officer Basin. A correlative is interpreted beneath the Bulldog Shale in GOMA DH3. Misspelt as the Pyndin Formation on p28.|c. 820 Ma|Callanna Group||Overlain by the Alinya Formation.||24-MAR-21
26843|Pindyin Sandstone|73090|5|Briefly described|Appendix.|Neoproterozoic|Neoproterozoic||||||Basal conglomerate, coarse-grained and gritty sandstone, cross-bedded, overlain by shale with chert beds, limestone and dolomite.|
26843|Pindyin Sandstone|73099|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Officer Basin.||||Is overlain by Alinya Formation.|Medium brown to dark red-brown, silty, very fine- to very coarse-grained, feldspathic quartz sandstone.|
26843|Pindyin Sandstone|73100|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Subsurface. Appears in the Legend as included in CALLANNA/BURRA GROUP EQUIVALENTS (mapped as one unit), but it is not specified to which Group it belongs.||||||
26843|Pindyin Sandstone|73109|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Is included in a map unit presented as Callanna/Burra Group equivalents that are mapped as one unit. Which Group contains it is not mentioned. Subsurface.||||||
26843|Pindyin Sandstone|73111|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Subsurface.||||||
26843|Pindyin Sandstone|73392|6|Mentioned|p3||||||||Sampled from core of Giles 1 well.|
39296|Pine Creek Kimberlite|24287|6|Mentioned|p30|||||||||
39296|Pine Creek Kimberlite|24584|5|Briefly described|p14, p19|Jurassic|Jurassic|Diatremes. Age: 174Ma (K-Ar date on phlogopite, Stacke et al 1979). Anomalous kimberlite; sub-outcropping. See also p15. See also Pine Creek kimberlites.||||||
76225|Pinyatta Member|72429|3|Fully described|p952, p956, p965-966|Lower Cambrian|Lower Cambrian|Mount Chambers Gorge, eastern Flinders Ranges. Up to 46m thick in measured section. Basal unit of the Moorowie Formation. Accessible outcrop means there are many sections measured. Shows evidence for episodic strong currents. Carbonate clasts are consistent with derivation from disaggregated archaeocyath skeletons. Fossil archaeocyaths and brachiopods are present in limestones. The depositional environment is interpreted to have been an archaeocyath meadow or bioherm, located in well-oxygenated clear waters on an open shelf marine environment, with light to moderately active currents and strong sunlight. Records the first major pulse of the proposed marine regression in the Mt Daily area.||Moorowie Formation||Overlies the Mernmerna Formation. Underlies the Wookata Shale Member.|Massive, thick-bedded, buff or pink to light grey, silty to sandy peloidal limestones with abundant archaeocyaths, cross-bedded quartz granule lenses, and ripple marks.|
39078|Pitjantjatjara Supersuite|60678|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Includes: Pottoyu Suite, Amputjuta Dacite, Manturrur and Umutju Suites, Walal Granite, Kulpitjata Suite, Ayers Range Granite, Kulgera Granite and the Umbeara granites.  Age: 1190-1120Ma. Geological Province: Musgrave Block.||||||
39078|Pitjantjatjara Supersuite|60679|5|Briefly described|Map Legend|Stenian|Stenian|Age: 1190-1120 Ma. Predominantly granites with some other similar rocks. Geological Province: Musgrave Block.||||||14-JAN-05
39078|Pitjantjatjara Supersuite|61154|2|Defined|p42 App., p9, p26-27|Mesoproterozoic|Mesoproterozoic|Comprises extensive suites of geochemically related granite bodies: Pottoyu, Umutju, and Kulpitjata Suites, Ayers Range and Kulgera Granites, Mantarurr Suite, Wala Granite(NT); and, Ernabella Adamellite suite, Ngarinya Adamellite(SA).  Age: ~1190-1120Ma.||||||03-AUG-05
39078|Pitjantjatjara Supersuite|61524|5|Briefly described|p16, p17 Fig.1, p18 Fig.2(a)|Mesoproterozoic|Mesoproterozoic|Felsic intrusives - alkali granite to diorite, almost exclusively charnockite in mapping area; undeformed to strongly deformed. Intrudes Birksgate Complex. Previously known as the Kulgara Suite. Age: 1170-1120Ma. Geological Province: Musgrave Province.||||||03-MAY-13
39078|Pitjantjatjara Supersuite|61864|5|Briefly described|p18, p19 fig 5|||Part of the basement of Musgrave Province. Associated with Musgravian Orogeny.|||||Granitic plutons; charnockitic and microgranite compositions.|
39078|Pitjantjatjara Supersuite|63224|5|Briefly described|p9||Mesoproterozoic|Elongated intrusive bodies. Geological Province: Beadell Province.||||||07-FEB-08
39078|Pitjantjatjara Supersuite|63776|6|Mentioned|p1089|Mesoproterozoic|Mesoproterozoic|Age: 1200-1140Ma. Voluminous granites.||||||
39078|Pitjantjatjara Supersuite|63864|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Age: c. 1155Ma or 1186-1164Ma. Charnockite; orthopyroxene-clinopyroxene metamonzogranite weakly, strongly and massively foliated. See map legend for more information.||||||
39078|Pitjantjatjara Supersuite|63866|5|Briefly described|p202, p206-p207|||Musgrave Province. Previously known as the Kulgera Supersuite.|c. 1190-1120 Ma||Includes the Pottoyu Suite, Umutju Suite, Walal Granite, Kulgera Granite, Umbeara Granite, Mantarurr Suite and the Kulpitjata Suite.||Alkali granite to diorite and extensive biotite granite gneiss.|
39078|Pitjantjatjara Supersuite|64408|5|Briefly described|map legend|Mesoproterozoic|Mesoproterozoic|Two dates shown: 1171-1180 Ma, 1194-1215 Ma. Not clear what was dated. Subdivided into 2 named & 11 unnamed units. Geol.  Province - Musgrave Complex.||||||16-SEP-08
39078|Pitjantjatjara Supersuite|64645|5|Briefly described|p16 Fig. 2|Mesoproterozoic|Mesoproterozoic|Age: 1200 - 1140Ma. Geological Province: Musgrave Province.||||||
39078|Pitjantjatjara Supersuite|64722|5|Briefly described|Fig. 2 p3-6, p17, 27|Stenian|Stenian|Of the Musgrave Orogen. Syn- to post-tectonic. Has within-plate, A-type affinities. Subjected to amphibolite-granulite facies metamorphism.|U-Pb zircon ages of ~1200-1120 Ma.||||Granite to diorite composition.|11-APR-12
39078|Pitjantjatjara Supersuite|64745|5|Briefly described|p375, p370, p373 Fig. 3, p374 Tab.1|||Voluminous emplacement of granitic rocks: adamellite to diorite composition, commonly porphyritic. A-type granites. Age: ca. 1.12 - 1.14Ga (U-Pb SHRIMP). Geol. Prov: Musgrave Province.||||||
39078|Pitjantjatjara Supersuite|64831|5|Briefly described|p1128 Fig. 2, p1129 Fig.3|Mesoproterozoic|Mesoproterozoic|Granitoid plutons ranging from alkali granite to quartz diorite in composition; contains microgranite and charnockite bodies. Magmatism was active from ca 1200Ma to 1150Ma (SHRIMP). See also pages 1130, 1135.||||||10-FEB-09
39078|Pitjantjatjara Supersuite|65135|4|Described|p1, p6 Fig.4, p12-13, p12 Fig.8, p16-18|Stenian|Ectasian|Most abundant in the northeast of west Musgrave Complex, but only forms small plutons and dykes in the southwest. Voluminous A-type granites. Broadly charnockitic. Metamorphosed to granulite facies. Preserves rapakivi textures in low strain zones. Divided into 2 main age groups: 1219-1200 and 1190-1155 Ma. Syn- to post-tectonic. Intruded by Alcurra Dolerite.||||||
39078|Pitjantjatjara Supersuite|65376|6|Mentioned|p9 Fig.1.2. |Mesoproterozoic|Mesoproterozoic||||||Granitic rocks.|
39078|Pitjantjatjara Supersuite|65385|5|Briefly described|pS131 Tab.2, pS132|Stenian|Stenian|Synorogenic granites. Of Musgrave Province. Intruded Birksgate Complex between 1190-1120 Ma.||||||08-MAR-12
39078|Pitjantjatjara Supersuite|65693|6|Mentioned|p3 Fig.1.|||Includes mafic dykes dated c.1149 Ma.||||||
39078|Pitjantjatjara Supersuite|65833|5|Briefly described|p1, p6 Fig.4, p12 Fig.8, p12-13, p16-18|Stenian|Stenian|Voluminous A-type granites. Rapakivi textured. Primary mineralogy includes orthopyroxene, pyroxene and biotite. Syn- to post-tectonic (Musgravian Orogeny); granulite facies metamorphism. Two major episodes of magmatism and metamorphism: 1219-1200 Ma and 1190-1155 Ma. Dated granites range from 1219 +/- 12 Ma (Bodorkos et al., 2008) to 1164 +/- 10 Ma (GSWA preliminary data). Mafic dykes intrude Musgrave Complex.||||||
39078|Pitjantjatjara Supersuite|65898|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Musgrave Province. Authors separate this into 2 unnamed Early (1219-1190 Ma), 4 unnamed Late (1190-1155 Ma) units and an ungrouped ?younger unit. Metagranites and gneiss. Also misspelt on Interpreted Bedrock Geology Figure as Pitjantjatjarra Supersuite.||||||
39078|Pitjantjatjara Supersuite|65906|6|Mentioned|p3, p5|Mesoproterozoic|Mesoproterozoic|Large proportion of outcrop in Musgrave Block. Age: 1220-1140 Ma. Produced by magmatism associated with the Musgravian Orogeny. Diorite to monzonite; within-plate, A-type affinities.||||||
39078|Pitjantjatjara Supersuite|65907|5|Briefly described|p5, p10, p13, pp26-27.|||Syn- to post-tectonic granitic intrusions; A type; metamorphosed to granulite facies. Two distinct age groups, defining Early and Late Musgravian Orogeny. |c.1219-1200 Ma, and c.1190-1155 Ma.|||||
39078|Pitjantjatjara Supersuite|66256|4|Described|p4 Fig.3, p6, p8-11, p13, see comments|Stenian|Ectasian|In west Musgrave Province. Edgoose et al. (2004) grouped syn- to post-tectonic granite magmas (of Musgrave Orogeny) into Pitjantjatjara Supersuite. Supersuite can be subdivided into eight suites based on geochemical similarities within groups of similar age and limited geographical extent. All rocks have been recrystallized at granulite facies. Granite geochemistry (whole-rock geochemical, Nd and Hf isotopic analyses) provided. Geochron (SHRIMP) results for crystallisation and metamorphic ages detailed. See also  p15-18, p23 Figs.20&21, p24-32, p34-47, p53-54 App.1, p71 App.4.|||Mirturtu, Ilurpa, Walpa, Waratjarra, Pirntirri, Punuwarra, Tjuni Purlka, Kapi-Parra suites.||3 granite groups: monzodiorite to alkali-feldspar granite; locally schlieric, biotite-orthopyroxene monzogranite to syenogranite; locally derived anatectic melts - highly leucocratic sheets and veins; depleted in REE and HFSE, enriched in LILE.|11-JAN-17
39078|Pitjantjatjara Supersuite|66280|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Musgrave Province. Divided on map into early (c.1219-1190 Ma, monzodiorite; leucogranite) and late (c.1190-1155 Ma, leucogranite; syenogranite; more) Pitjantjatjara Supersuite as well as several mapped but unnamed units of metagranite and gneiss.||||||
39078|Pitjantjatjara Supersuite|66281|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Musgrave Province.|||||Metamonzogranites, granodiorites, metaleucogranites, metasyenogranites, mylonitic granitic rock.|
39078|Pitjantjatjara Supersuite|66282|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Musgrave Province. Metagranite and gneiss. Mapped as eleven lithologically-different but un-named units.|||||Weakly to strongly foliated metamorphosd monzogranite, syenogranite, porphyritic leucogranite, granofels, leucosyenogranite.|
39078|Pitjantjatjara Supersuite|66284|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Musgrave Province. Includes an early and a late phase, separated by Mirturtu Monzogranite; and 13 separately-mapped but un-named units.|c.1219 - 1155 Ma.||Includes Umutju Granite.||Includes metagranodiorite, metamonzogranite, gneissic porphyritic leucogranite, medium-grained mafic granulite, granitic gneiss, metasyenogranite.|
39078|Pitjantjatjara Supersuite|66526|5|Briefly described|p35.|Proterozoic|Proterozoic|Granitic rocks. They include a dated gabbro intrusion and associated mafic granulite produced in the Pitjantjatjara Event, ME 22 in the Proterozoic Mafic-Ultramafic Magmatic Event Series.|c.1180 Ma.|||||
39078|Pitjantjatjara Supersuite|67128|5|Briefly described|p5 Fig.3, p6-8, p15|||Walpa Pulka Zone, western Musgrave Province. Voluminous A-type felsic and minor mafic magmatism associated with the c.1220-1150 Ma Musgravian Orogeny.|c.1220-1150 Ma.|||Is overlain unconformably by MacDougall Formation.|Typically K-feldspar porphyritic granite plutons with ultra high-T metamorphic assemblages; local schlieric biotite-orthopyroxene leucogranites.|
39078|Pitjantjatjara Supersuite|67244|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Musgrave Province. Mapped as four separate but un-named sub-units. Informally grouped into an unnamed unit and an older 'Late Pitjantjatjara Supersuite' (1190-1150) grouping of 3 unnamed units.|>1150 Ma.||||Metagranodiorite intercalated with pelitic gneiss and olivine gabbro; mylonitic, seriate to porphyritic metagranitic rock; foliated biotite-hornblende metasyenogranite with locally abundant xenoliths of felsic gneiss.|01-MAY-15
39078|Pitjantjatjara Supersuite|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Musgrave Block.|~1190-1120 Ma.|||||
39078|Pitjantjatjara Supersuite|67372|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Musgrave Province. Mapped as no fewer than 40 separate but un-named (except for the 2 units comprising the Mirturtu Suite) units.|1220 - 1150 Ma.||Includes Mirtutu Suite.||40 mapped units of variably-metamorphosed leucogranite, granodiorite, monzogranite, syenogranite, granite, olivine gabbro, monzodiorite and charnockite; pelitic gneiss; mafic granulite.|02-DEC-13
39078|Pitjantjatjara Supersuite|67375|3|Fully described|p6,Fig.5, p15, pp26-32, p58, pp150-213.|Mesoproterozoic|Mesoproterozoic|Of Edgoose et el. (2004); formerly the Kulgera Suite of Major and Conor (1993). Incorporates all igneous rocks formed during the Musgrave Orogeny, and anatectic melts as young as 1121 +/- 11 Ma resulting from high-grade metamorphism in the late stages of the Musgrave Orogeny. Most granites are metaluminous, K-rich, A-type. Enormous amounts of granitic magma, covering half the entire Musgrave Province. Most have been metamorphosed to granulite-facies, and range from statically recrystallized and unfoliated to strongly foliated and mylonitized. Is intruded by a tubular-shaped mafic-ultramafic chonolith which hosts the world-class Nebo-Babel Ni-Cu-PGE sulfide orebody.|1219 +/- 12 Ma - 1148 +/- 6 Ma.||Includes Tjuni Purlka Suite. Encloses xenoliths and rafts of Wirku Metamorphics. Intrudes Wankanki Supersuite.||Three groups: monzodiorite to alkali-feldspar granite dykes and small plutons; schlieric biotite-orthopyroxene leucogranite veins and sheets; locally derived anatectic melts, typically with granofelsic textures. Rare leucogabbro and norite.|
39078|Pitjantjatjara Supersuite|67536|5|Briefly described|Map Legend|Ectasian|Stenian|Musgrave Block. Informally subdivided into two parts. Possibly occurs in the Beadell Province as elliptical non-magnetic to weakly magnetic intrusive bodies, some with magnetic rims and N-trending magnetic lineations.|ca. 1200 - 1175 Ma ?||||Granitoid plutons and phases of larger plutons, non-magnetic to moderately magnetic; granitoid plutons, massive to internally zoned, including intrusive charnockite, strongly magnetic.|
39078|Pitjantjatjara Supersuite|67553|4|Described|p8-9,11-12,16-17,19-20-34,39,59,61|Mesoproterozoic|Mesoproterozoic|Geological province: Musgrave Province, North Australian Craton. High-K granitic plutons, dominant within the Walpa Pulka Zone, and covers roughly half of the entire Musgrave Province. Calc-alkaline to alkaline calcic 'charnockitic' magmatism at 1220-1150 Ma (Close et al., 2003; and GSWA data). Based on SHRIMP U-Pb geochronology, this can subdivided into two groups,  Early and Late Musgravian granites reflecting magmatism and metamorphism c. 1220 and 1200 Ma and c. 1190 and 1155 Ma respectively. Oldest and youngest Early Musgravian granites dated at 1219+\-12 Ma (GSWA 174737) and 1157+\-9 Ma (GSWA 189254) respectively. Most granites in the Mamutjarra Zone have late Musgravian intrusive ages between 1189+\-11 Ma (GSWA 184147, Kirkland et al., 2009d) and 1148+\-6 Ma (GSWA 189522, Kirkland et al., in prep.).  Granites in the Yjuni Purlka zone include deformed early Mugsgravian granites, similar Mamutjarra Late musgravian granites and schlieric biotite-orthopyroxene leucogranites ranging from 1210+\-10 Ma (GSWA 185339, Kirkland et al., 2009e) to 1165+\-10 Ma (GSWA 183509, Kirkland et al., 2008c). Most rocks metamorphosed to granulite-facies conditions late in Musgrave Orogeny and during Giles Event. Exhumation during Petermann Orogeny exposed deep metamorphic assemblages. Subdivisible into three main lithological components (see p28-30). See also p67,70-71,73-75,78,82,95 for general field trip notes.|1220-1150 Ma||Includes Mamut, Mirtutu, Kapi-Parra, Waratjarra, Pirntirri, Ilurpa, Walpa Punuwarra and Tjuni Purlka suites.||Monzodiorite to alkali-feldspar granite, locally schlieric biotite-orthopyroxene leucogranites (monzogranite to syenogranite) and locally derived anatectic melts forming highly leucocratic sheets and veins, typically with granofelsic textures.|
39078|Pitjantjatjara Supersuite|67581|6|Mentioned|p44 Fig.8|||||||||
39078|Pitjantjatjara Supersuite|68077|5|Briefly described|p3 Fig.1, p4-6, p11-14, p18-19, p30|Mesoproterozoic|Mesoproterozoic|See also p32-38. The Musgrave Orogeny produced these extensive, >1000 oC granites. Forms a sheet up to 5km thick. Isotopic composition (Lu-Hf and Sm-Nd) and evolution tabulated and discussed in detail.|1219-1180 Ma (U-Pb zircon)||||Charnockitic and locally rapakivi-textured granites, ferroan and typically alkali-calcic; pegmatites, metagranite, metagranodiorite, monzodiorite, gabbro and dolerite.|07-SEP-17
39078|Pitjantjatjara Supersuite|68100|5|Briefly described|p2, 3, 4-5, 7-9, 12,14,15,16,24-29,33,34|Mesoproterozoic|Mesoproterozoic|Leucogranites appear as magnetic lows. Metamorphosed to granulite facies ~1080-1030 Ma (Giles Event).|1220-1150 Ma||||K-feldspar porphyritic granites and minor mafic rocks. The granites are primarily anhydrous charnockites. Anatectic, garnetiferous, mylonitic leucogranites; gabbro.|19-JAN-17
39078|Pitjantjatjara Supersuite|68131|5|Briefly described|p2 Fig.1|Mesoproterozoic|Mesoproterozoic||||||Granitic rocks.|
39078|Pitjantjatjara Supersuite|68995|5|Briefly described|p2, p5, p6, p48, p50, p51 Tb. 4, p65|Stenian|Ectasian|Intruded during the Musgrave Orogeny. Interpreted to be mostly derived from a mantle source based on isotopic concentrations and thermal limits of intrusion.|c.1220-1150 Ma|||Unconformably overlain by the Kunmarnara Group.|Orthopyroxene-bearing and locally rapikivi textured granites.|
39078|Pitjantjatjara Supersuite|68996|5|Briefly described|p3, 4, 24-25, 28-30,35-49, 54, 59|Mesoproterozoic|Mesoproterozoic|Musgrave Orogeny granites. Densities range from 2.57-3.25g/cm^3|1220-1155 Ma||||High grade granitic gneisses and charnockites. Chemistry suggests within-plate, A-type magmatism.|
39078|Pitjantjatjara Supersuite|68998|6|Mentioned|p31|||Musgrave Province. Mentioned as a significant source of zircons in the Mount Eclipse Sandstone.||||||
39078|Pitjantjatjara Supersuite|69003|5|Briefly described|p4, p37-39, p42-43, p45, p51|Mesoproterozoic|Mesoproterozoic|W Musgrave Province, Paterson Orogen. Associated with the 1220-1150 Ma Musgrave Orogeny.|1220-1150 Ma.||Tjuni Purlka suite.||Voluminous, anhydrous, orthopyroxene-bearing felsic magmatic rocks; mainly composite plutons ranging from monzodiorite through to alkali-feldspar granite, including significant rapakivi granite. Mafic rocks are extremely rare.|
39078|Pitjantjatjara Supersuite|69009|5|Briefly described|Map Legend|Stenian||Musgrave Province.|> 1078 Ma||||Comprises metagranite and gneiss.|03-APR-14
39078|Pitjantjatjara Supersuite|69091|4|Described|p52 Fig.4.1, p53, see comments|Mesoproterozoic|Mesoproterozoic|Formed during 1220-1150 Ma Musgrave Orogeny. West Musgrave Province. Mount West Orogeny and Musgrave Orogeny, including mixed with Wankanki Supersuite (Fig.4.3). In Wannarn area, Kunmarnara Group are interleaved with felsic basement, including granulite facies metagranites of Pitjantjatjara Supersuite. See also p54-56, p59 Fig.4.6, p64-67, p82-83, p85-88, p103 Fig.5.6, p105-107, p109 Fig.5.10, p113-115, p117 Fig.5.15, p119 Fig.5.16, p121, p131-132, p137-139 Figs.6.4-6.6, p141-142, p151, p183-184, p206.|1220-1150 Ma||Tjuni Purlka, Kapi-Parra, Mamut, Mirturtu, Pirntirri, Ilurpa and Waratjarra suites; Pottoyu Granite Suite.|Is unconformably overlain by Kunmarnara and Tjauwata Groups.|High-K granite plutons; most metamorphosed granulite-facies; granites range from statically recrystallised and unfoliated, to strongly foliated and mylonitised; includes high-grade granitic gneisses and charnockites; suggests A-type magmatism.|
39078|Pitjantjatjara Supersuite|69153|5|Briefly described|GEOL_LUT_CSV files;GEOCHRON/194637.1.pdf|Mesoproterozoic|Mesoproterozoic|Paterson Orogen, Musgrave Province. Some of this unit is divided into subparts: Pitjantjatjara Supersuite 1 and Pitjantjatjara Supersuite 2. Age mentioned in GEOCHRON/194637.1.pdf.|1220-1150 Ma, Smithies et al., 2010||Umutju Granite (in sub-part Pitjantjatjara Supersuite 2)||Metagranodiorite, metasyenogranite, metamonzogranite, granitic schist, granitic granofels/hornfels, mafic granulite, granitic gneiss;  intercalated with, intruded by, and included in other granitic rocks|
39078|Pitjantjatjara Supersuite|69203|5|Briefly described|p59|||Musgrave Province.|c.1190-1120 Ma.||||Voluminous I-type magmatism.|
39078|Pitjantjatjara Supersuite|69213|6|Mentioned|p36, p35|||Musgrave Province.|~1200-1140 Ma||||Anhydrous charnockites.|
39078|Pitjantjatjara Supersuite|69383|6|Mentioned|p74, 77|||Musgrave Province.|1190-1120 Ma|||||
39078|Pitjantjatjara Supersuite|69417|6|Mentioned|p2:10|Mesoproterozoic|Mesoproterozoic|Granitoids, interpreted to have formed by the extensional Musgrave Orogeny.||||||12-JUL-16
39078|Pitjantjatjara Supersuite|69436|4|Described|p21:1-2, 4-10, 15-18, 21|Mesoproterozoic|Mesoproterozoic|Musgrave Province. Voluminous widespread syn- to post-tectonic granitic magmatism, synchronous with the Musgrave Orogeny (1220-1150 Ma). Extensively reworked by the Petermann Orogeny with pervasive biotite foliation. Peak metamorphic assemblages include biotite-epidote-muscovite +/- garnet. Three metamorphic zircon rims have ages between 574 +/- 5 Ma and 568 +/- 12 Ma. Has some potential for iron oxide-Cu-Au deposits.|1220-1120 Ma.||Pottoyu, Umutju, Mantarurr, Kulpitjata Suites; Walal, Ayers Range, Kulgera Granites.||Comprises extensive Suites of geochemically related granite bodies, from diorite to granite, generally subalkaline and predominantly ultrapotassic, although some are high-K calc-alkaline types. Metaluminous I-type.|12-JUL-16
39078|Pitjantjatjara Supersuite|69640|4|Described|p11-p12, p15, p23-p24, p27|Proterozoic|Proterozoic|Musgrave Province. Petrology, petrographic description, SHRIMP methodology, results and analayses for numerous samples are provided. Additional magmatic crystallisation ages of 1147 +/- 11 Ma,1147 +/- 16 Ma, 1143 +/- 9 Ma,  1143 +/- 8 Ma, 1155 +/- 14 Ma and 1152 +/- 9 Ma were obtained by SHRIMP. Also includes medium-grained equigranular granite with pegmatite with a rough ca 1140 Ma magmatic age and a biotite micro-syenogranite dyke dated at 1154 +/- 9 Ma. See also  p32, p50, p82, p88, p94, p100, p107, p115, p122, p130, p137, p141, p145, p148, p152, p157, p164, p174, p190, p207, p214.|1564 +/- 5 Ma (SHRIMP, magmatic crystallisation)|||Intruded by the Alcurra and Kullal dolerites. Intrudes the Birksgate Complex.|Anatectic granites, plutonic A type porphyritic granites and late crosscutting microgranitic and aplitic dykes. Porphyritic biotite monzogranite,  biotite monzogranite dykes, biotite micro-monzogranite,  monzodiorite.|
39078|Pitjantjatjara Supersuite|69655|5|Briefly described|p3, p5-p7, p9, p37|Stenian|Ectasian|See also p39, p44, p57-p58, p66, p77-p78. Musgrave Province. Musgrave Orogeny.|c. 1220-1150 Ma||||Orthopyroxene-bearing and locally rapakivi granites.|
39078|Pitjantjatjara Supersuite|69729|4|Described|p66-70, p74-78, p84-85, p87-88, p90|Mesoproterozoic|Mesoproterozoic|Edgoose et al. (2004). Musgrave Province. Emplaced during the Musgrave Orogeny. Geochemistry detailed. UHT conditions discussed.|1220-1150 Ma.|||Cross-cuts and encloses Wirku Metamorphics and Wankanki Supersuite.|Almost exclusively felsic, high-temperature, anhydrous, A-type, high-K, granulite facies metagranites.|
39078|Pitjantjatjara Supersuite|69917|5|Briefly described|p115|Mesoproterozoic|Mesoproterozoic|Musgrave Province. Granites of  1190-1120 Ma.||||||
39078|Pitjantjatjara Supersuite|69937|5|Briefly described|vi, p7, p9, p12, p19, p22, p27, p31|||Musgrave Province. One of the sediment sources for the Amadeus Basin.|1220-1120 Ma.||||Granites.|
39078|Pitjantjatjara Supersuite|70083|6|Mentioned|p204, 206-208, 226, 229, 231-232|||Musgrave Inlier. Associated with widespread amphibolite-granulite facies metamorphism of the Musgrave Orogeny. Magnetic anomalies support a connection with contemporaneous Nornalup Complex granites (Albany-Fraser Orogen) and Teapot [Granite Complex] granites (Warumpi Province).|~1220-1140 Ma.||||Voluminous A-type felsic magmatic rocks: felsic granitoids and microgranitic dykes.|
39078|Pitjantjatjara Supersuite|70084|4|Described|p219-225,228-229|Stenian|Ectasian|Geological province: Musgrave Province, Paterson Orogen. Associated with Musgrave Orogeny, coeval with emplacement of Esperance Supersuite and Gnowangerup Fraser Dyke Suite in the Albany-Fraser Orogen. Voluminous granitic magmatism accompanied by UHT metamorphic conditions (associated with unusually thin crust and extreme geothermal gradients), and one of the largest exposed UHT belts on Earth. Granitic composition described from Smithies et al., 2011. Lies within a single, narrow, Nd and Hf-isotopic evolution band with TDM2 values within a range of 2.2-1.6 Ga, together with the Wankanki, Papulankutja and Warlawurru supersuites, reflecting reworking of juvenile crust between ca. 2.0 and 1.6 Ga (Kirkland et al., 2013a). Mid-crustal accummulation of high Th, U and K-rich granites resulted in slow post-Musgrave Orogeny thermal decline, consistent with prolonged migmatite events (Smithies et al., 2014a).|1220-1150 Ma||||Almost exclusively felsic, anhydrous, A-type granites (ferroan, typically alkali-calcic (high-K) and range in silica content from 56.8 to 78.0 wt%, with very high concentrations of both TiO2 and P2O5 and enrichments in REE, HFSE, Th, and U.|
39078|Pitjantjatjara Supersuite|70134|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Musgrave Province.|||||Metagranite and gneiss (section only).|
39078|Pitjantjatjara Supersuite|70338|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Part of the basement of the Musgrave Province. Seven facies are mapped separately. Lithologies are described in a little more detail.|||||Undivided: adamellite, alkali granite, diorite. Micromonzogranite to microsyenogranite; microsyenogranite; syenogranite to quartz-monzodiorite; metasyenogranite to metaquartz-monzodiorite; monzogranite to syenogranite: porphyritic or equigranular.|07-JAN-16
39078|Pitjantjatjara Supersuite|70383|6|Mentioned|p51|Stenian|Stenian|Musgrave Province. Mentioned as a possible source of zircons aged c.1178 +/- 15 Ma, extracted from the Sprigg Diamictite Member.||||||
39078|Pitjantjatjara Supersuite|70619|5|Briefly described|map legend|Mesoproterozoic|Mesoproterozoic|Musgrave Province.|1219-1148 Ma||||Metagranite and gneiss.|
39078|Pitjantjatjara Supersuite|70634|4|Described|100k_geologyp_lut,csv|Mesoproterozoic|Mesoproterozoic|Musgrave Province/(Complex?), SHRIMP dates obtained from samples (file 174558.1.pdf,   194802.1.pdf)|1134Ma (SHRIMP) -   1215 Ma (SHRIMP)|Musgrave Complex|Includes Mirturtu Suite, Umutju Granite, Mirturtu Monzongranite Suite|Intruded by Warakurna Supersuite|Hornblende--biotite--pyroxene metasyenogranite and metamonzogranite, leucogabbro, quartz diorite, feldspar porphyritic charnockite.|
39078|Pitjantjatjara Supersuite|70748|6|Mentioned|p15, p50|||Musgrave Province. Similar in age to the Eyre 1 granite.||||||25-SEP-18
39078|Pitjantjatjara Supersuite|70749|5|Briefly described|p50-51|||Emplaced during the Musgrave Orogeny.|||||Widespread and voluminous felsic intrusions.|
39078|Pitjantjatjara Supersuite|70763|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Musgrave Province. Associated with the Musgrave Orogeny. Three facies are mapped separately.|1219-1148 Ma.||||Three facies mapped separately: metagranite and gneiss; hornblende-biotite metamonzogranite and biotite-hornblende metamonzogranite, both well-foliated to gneissic, garnet-bearing, locally migmatitic.|
39078|Pitjantjatjara Supersuite|70778|6|Mentioned|p21|||Musgrave Province. Emplaced during the Musgrave Orogeny.||||||
39078|Pitjantjatjara Supersuite|70793|4|Described|GEOL_LUT_CSV files + geochron files|Mesoproterozoic|Mesoproterozoic|Geological province: Paterson Orogen, Musgrave Province. Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma); Giles Event (1085-1040 Ma); Musgrave Orogeny (1220-1150 Ma). Sample GSWA 174558 (quartz diorite) yielded an interpreted igneous crystallisation age of 1145+\-12 Ma (weighted mean 207Pb*/206Pb*). Sample GSWA 174594 (metaleucograbbro) yielded an interpreted (weighted mean 207Pb*/206Pb*) igneous crystallisation age of 1190+\9 Ma. Sample GSWA 174736 (granofelsic metasyenogranite) yielded an interpreted (weighted mean 207Pb*/206Pb*) igneous crystallisation age of 1180+\7 Ma. Sample GSWA 174737 (foliated metamonzogranite) yielded an interpreted (weighted mean 207Pb*/206Pb*) igneous crystallisation age of 1219+\12 Ma, and metamorphic zircon rim growth at 1171+\-12 MA. Sample GSWA 174747 (metagabbro) yielded an interpreted (weighted mean 207Pb*/206Pb*) maximum igneous crystallisation age of 1205+\-24 Ma, and metamorphic zircon rim growth at 1214+\-7 Ma. Sample GSWA 180262 (mylonitic synogranite) yielded an interpreted (weighted mean 207Pb*/206Pb*) igneous crystallisation age of 1180+\-4 Ma. Sample GSWA 180270 (metamonzogranite dyke) yielded an interpreted (weighted mean 207Pb*/206Pb*) igneous crystallisation age of 1183+\-9 Ma. Sample GSWA 180860 (metamonzogranite) yielded an interpreted (concordia) igneous crystallisation age of 1159+\-13 Ma. Sample GSWA 183459 (charnockite) yielded an interpreted (weighted mean 207Pb*/206Pb*) magmatic crystallisation age of 1178+\-12 Ma. Sample GSWA 183509 (leucogranite) yielded an interpreted (weighted mean 207Pb*/206Pb*) magmatic crystallisation age of 1165+\-10 Ma. See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop14_lut.csv, 100k_interpgeol_lut.csv, 500k_interpgeop_lut.csv, 100k_geologyl_lut.csv, 250k_interpgeol_lut.csv, 2_5m_interpgeop15_lut.csv, 500k_interpgeol_lut.csv + geochron files for more geochronological sample analyses.|1219+\-12 Ma; 1148+\-6 Ma||Includes Mirturtu Suite, Pottoyu Granite Suite, Umutju Granite Suite.|Intruded by Warakurna Supersuite. Intrudes into Wirku Metamorphics.|Mafic granulite, granitic gneiss, metasyenogranite and metamonzogranite, granulite, metagranite and gneiss, leucocratic syenogranite, metaleucosyenogranite.|
39078|Pitjantjatjara Supersuite|70826|6|Mentioned|p10|Mesoproterozoic|Mesoproterozoic|Musgrave Province. ||||||
39078|Pitjantjatjara Supersuite|70831|5|Briefly described|p1, p3-p4, p6, p9, p13-p15, p20-p21, p23|Stenian|Ectasian|Musgrave Province. Average mineralogy is discussed. Petrography of constituent samples is discussed.|c. 1220-1150 Ma||||Well-foliated to gneissic, garnet-bearing, biotite-hornlende metamonzogranites.|
39078|Pitjantjatjara Supersuite|70839|5|Briefly described|p326-327,332,334,339-341,345|Stenian|Ectasian|Geological province: Musgrave Province. Dominates the Musgrave Province in outcrop. Emplaced between c. 1.22 and 1.15 Ga during Musgrave Orogeny (Smithies et al., 2011).|c. 1220-1150 Ma|||||
39078|Pitjantjatjara Supersuite|70968|5|Briefly described|p130|||Mentioned as possible source of detrital zircons in post-Roper Group units in greater McArthur Basin.|1220-1120 Ma.|||||
39078|Pitjantjatjara Supersuite|71088|5|Briefly described|p2, p4-p5, p7, p10, p25|Mesoproterozoic|Mesoproterozoic|Musgrave Province. Emplaced during the Musgrave Orogeny; an extensional and intracontinental event characterised by ultra-high temperatures.|1220-1150 Ma||||Granites.|
39078|Pitjantjatjara Supersuite|71143|5|Briefly described|p433,437|||Geological province: Musgrave Province. Similar age and composition to orthopyroxene- and pigeonite-bearing monzogabbro to monzodiorite rocks found from the Moodini Supersuite in the Madura Province (includes juvenile mantle input).||||||
39078|Pitjantjatjara Supersuite|71169|6|Mentioned|p82|Stenian|Ectasian|Musgrave Province. |1220-1120 Ma|||||
39078|Pitjantjatjara Supersuite|71170|5|Briefly described|xi-xii, p5-p6, p9, p42-p43|Mesoproterozoic|Mesoproterozoic|Musgrave Orogen. Emplaced at high temperatures (>900c). See also p45, p65-p67, p109, p145, p147.|1220-1150 Ma (Smithies et al, 2010)||||Charnockitic, A-type granitic rocks.|
39078|Pitjantjatjara Supersuite|71210|6|Mentioned|p4-p5, p7-p8, p21, p23, p51, p53|||Musgrave Province. See also p66-p67, p69, p78-p82, p86, p95-p97, p99, p113. Also appears as Pitjantjatjara Supergroup p8.||||Overlain by the Kunmarnara Group.||
39078|Pitjantjatjara Supersuite|71211|5|Briefly described|p6, p7 fig 1.4, p9, p24 fig 2.1|||Musgrave Province. See also p84 fig 3.1, p104, p106, p107, p136 fig 4.1 , p230. |1220-1150 Ma||||Granites.|
39078|Pitjantjatjara Supersuite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||granite|
39078|Pitjantjatjara Supersuite|71268|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Geological Province: Paterson Orogen, Musgrave Province. Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma); Giles Event (1085-1040 Ma); Musgrave Orogeny (1220-1150 Ma). Metamorphosed to granulite facies, with garnet-biotite rims around zircons indicating cooling post-peak metamorphism. Sample GSWA 174558 (mesocratic quartz diorite) yielded a weighted mean 207Pb/206Pb date of 1215+\-13 Ma, interpreted as the igneous crystallization age of the quartz diorite. Sample GSWA 174594 (plagioclase leucogabbro) yielded a weighted mean 207Pb/206Pb date of 1190+\-9 Ma, interpreted as the igneous crystallization age of the leucogabbro. Sample GSWA 174736 (granofelsic metasyenogranite) yielded a weighted mean 207Pb/206Pb date of 1180+\-7 Ma, interpreted as the igneous crystallization age of the syenite. Sample GSWA 174737 (foliated monzogranite) hosts the syenite, and is dated at 1219+\-12 Ma, and contains metamorphic zircon growths at 1171+\-12 Ma. These relationships suggest that syenogranite emplacement was broadly synchronous with the high-grade metamorphic event that affected the host monzogranite. Sample GSWA 180262 (mylonitic syenogranite) yielded a weighted mean 207Pb/206Pb age of 1180+\-4 Ma, interpreted as age of igneous crystallization of the precursor syenogranite. Sample GSWA 184146 (monzogranite) yielded a concordia age of 1201+\-6 Ma, interpreted as magmatic crystallsiation age. See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 1m_geologyp12_lut.csv, 1m_geologyp12_lut.csv, 500k_interpgeop16_lut.csv, 100k_interpgeol_lut.csv, 100k_geologyl_lut.csv, 250k_interpgeol_lut.csv, 2_5m_interpgeop15_lut.csv, 500k_interpgeol_lut.csv.|1219-1148 Ma (inferred)||Includes Permano Adamellite, Mirtutu Suite, Pottoyu Granite Suite, Umutju Granite Suite.|Overlain by Tjauwata Group.|Granite, monzogranite, monzonite, granodiorite. Includes metagranodiorite, metamonzogranite, gneissic porphyritic leucogranite, medium-grained mafic granulite, granitic gneiss, metasyenogranite.|
39078|Pitjantjatjara Supersuite|71302|5|Briefly described|p75|Mesoproterozoic|Mesoproterozoic|Geological province: Musgrave Province. Voluminous granitic magmatism at c. 1220-1120 Ma.||||||
39078|Pitjantjatjara Supersuite|71321|4|Described|p1-2,4-5,10,14,17-19,21,24|Stenian|Stenian|Geological province: Musgrave Province. Voluminous, felsic, A-type granitoids synchronous with, and post-dating Birksgate Complex deformation during c. 1155 Ma Musgravian Orogeny. Form several large plutonic bodies distributed over TIEYON and dominate the basement outcrop exposure of the map sheet. Plutons also show magmatic foliation as a result of Musgravian Orogeny. Also contains locally developed, ductile to brittle structures (i.e. mylonites, schistosity, and joints) which may be attributed to Neoproterozoic-Cambrian Petermann Orogeny. Broadly grouped into 3 suites based on lithology, geochemistry and field relationships; anatectic granite suite, plutonic granite suite (intrudes into anatectic suite) and microgranite dyke suite (intrudes into both anatectic and microgranite suites). See p18-22 for detailed lithological and petrographic descriptions and field relationships in outcrop. See p40-49 for detail geochemistry breakdown and analysis. Plutons emplaced between c. 1155-1143 Ma (average c. 1148.1+\-2.4 Ma). Anatectic granite suite may have been produced by melting of Birksgate Complex basement rocks. Nd isotopic analysis indicate the anatectic and porphyritic granitic suites overlap in isotopic signatures with the Birksgate Complex, while the microgranitic suite is the most evolved. Hf isotopic analysis indicate reworking of older Birksgate crust with addition of new juvenile mantle material, while the microgranite suite reflects mixing of evolved Archean source with juvenile Birksgate basement. Contains anomalous hydrothermal related Ag-REE mineralisation. See also p32-36,38,40-50,55-56,60-64,66,74.|c. 1155-1143 Ma|||Intrudes into Birksate Complex.|Adamellite; alkali granite; diorite; often porphyritic, foliated or even massive.|24-OCT-19
39078|Pitjantjatjara Supersuite|71322|5|Briefly described|p11, p26, p33|||Musgrave Province. Age range c.1220-1150 Ma, with ultra-high temperatures persisting to c.1120 Ma. Metamorphosed at 1156 +/- 9 Ma.|1219 +/- 9 Ma (SHRIMP).||||Includes charnockitic granite.|13-DEC-21
39078|Pitjantjatjara Supersuite|71415|6|Mentioned|p16|Mesoproterozoic|Mesoproterozoic|Geological province: Musgrave Province.||||||19-AUG-19
39078|Pitjantjatjara Supersuite|71416|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Solid geology interpretation: monzogranite to syenogranite plutons; early stage moderately to strongly magnetic, massive to weakly foliated, mainly medium-grained, equigranular to sparsely K-feldspar-phyric, commonly leucocratic; late stage strongly magnetic, massive to weakly foliated, medium- to coarse-grained, porphyritic. SHRIMP U-Pb zircon magmatic crystallisation age.|c.1150 Ma (Dutch et al., 2013).||||Porphyritic granite to monzonite, biotite and/or hornblende, rare clinopyroxene, locally inequigranular.|
39078|Pitjantjatjara Supersuite|71536|5|Briefly described|p1, p71, p73, p78|Stenian|Stenian|SHRIMP age derived from this volume and interpreted as the magmatic age of a felsic gneiss from this supersuite.|1143 +/- 9 Ma (U-Pb SHRIMP)||||Peraluminous granite derived from melting of a pre-existing sedimentary rock (probably Birksgate Complex).|
39078|Pitjantjatjara Supersuite|71592|5|Briefly described|Appendix A.|||Musgrave Province.|1190+/-9 Ma (crystallisation: U-Pb zircon SHRIMP)||||Metamorphosed leucogabbro, metagabbro, monzogranite, pegmatite, quartz monzodiorite, syenogranite, monzonite, granite, coarse-grained leucogranite, charnockite, granoblastic garnetiferous granite, biotite-hornblende granite.|
39078|Pitjantjatjara Supersuite|71800|5|Briefly described|p29|Mesoproterozoic|Mesoproterozoic|Musgrave Province. The probable source of sediments in the Officer and Amadeus basins on the basis of geochronology.|1.22-1.15 GA|||||
39078|Pitjantjatjara Supersuite|71893|5|Briefly described|p44, p48, p51|||Musgrave Province.|ca. 1220-1120|||||
39078|Pitjantjatjara Supersuite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoproterozoic|Mesoproterozoic|Musgrave Province, Paterson Orogen.|Max age 1219+/-12 Ma, min age 1148+/-6 Ma.||Includes Umutju Granite Suite, Pottoyu Granite Suite, and informal Pitjantjatjara Supersuite 1, Pitjantjatjara Supersuite 2.||Metagranite and gneiss. Mylonitic and blastomylonitic, seriate to porphyritic granitic rock. Mylonitic, medium-grained, porphyritic metamonzogranite; K-feldspar phenocrysts up to 2 cm.|
39078|Pitjantjatjara Supersuite|72094|5|Briefly described|p2, p3, p6, 12, 13, 14, p15-16|Stenian|Ectasian|Musgrave Province. Emplacement associated with Musgrave Orogeny, which metamorphosed Warlawurru, Papulankutja, Wankanki supersuites and Wirku Metamorphics to UHT (Edgoose et al., 2004; Smithies et al., 2010). Summary table of zircon geochronology on p8 Table 1 showing ages ranging from 1171+/-4 Ma to 1157+/-9 Ma.|1219-1148 Ma|||Tectonically interleaved with Kunmarnara Group along with Warlawurru Supersuite.|Metagranite and orthogneiss.|
39078|Pitjantjatjara Supersuite|72238|5|Briefly described|p36, 38|Mesoproterozoic|Mesoproterozoic|Geological province: Musgrave Province. Includes 1.15 Ga granites. Intruded by Amata Dolerite.|||Includes Wallaby Rock pluton, crosscut by Amata Dolerite.|||17-SEP-19
39078|Pitjantjatjara Supersuite|72242|5|Briefly described|p27|Stenian|Stenian|Geological province: Musgrave Province. Associated with Maralinga Event (including Musgrave Orogeny). Coeval with Moodini Supersuite.||||||
39078|Pitjantjatjara Supersuite|72443|5|Briefly described|p736-737, p747-748, p753, p758|Mesoproterozoic|Mesoproterozoic|Produced by the Musgrave Orogeny. Intrudes the  exposed mid-crust of the entire 1220-1150 Ma period. Interpreted to have been emplaced at temperatures of up to 1000 degrees C and coincided with a 100 Myr period of UHT metamorphism.|1220-1150 Ma||||Ferroan, alkali-calcic granites.|
39078|Pitjantjatjara Supersuite|72476|5|Briefly described|p25|||Eastern Musgrave Province.|1190-1120 Ma.||||Abundant high temperature granites.|
39078|Pitjantjatjara Supersuite|72934|6|Mentioned|p11-12|||Musgrave Province.|||||May include A-type granite intrusions.|
39078|Pitjantjatjara Supersuite|73058|5|Briefly described|p761, p769, p771 Fig.5-6, p773-776|Stenian|Ectasian|Musgrave Province. Ferroan and typically alkali-calcic granites, extreme enrichments in REE and HFSE. Intruded almost continuously throughout the Musgrave Orogeny as voluminous, high-temperature, anhydrous granites in mid-crustal regions, source dominated by new mantle additions. Hf and Nd model ages suggest mantle extraction event at c. 1900 Ma. Inferred additional significant juvenile mantle additions are masked in Hf isotope record by HFSE enriched crustal sources. Misspelt Pitjantatjara Supersuite p775. Location in text includes p772 Fig.8-9, p777 Fig.14.|c.1220-1150 Ma||||Includes orthopyroxene-bearing (charnockitic) and locally rapakivi-textured granites.|
39078|Pitjantjatjara Supersuite|73084|6|Mentioned|p12, p96, p98, p109, p124|Stenian|Ectasia|Musgrave Province. Similar in composition and age to the Moodini Supersuite and Esperance Supersuite. Part of a regionally extensive, high-temperature event named the Maralinga Event by Spaggiari et al. (2016).|1220-1150 Ma|||||
39078|Pitjantjatjara Supersuite|73177|5|Briefly described|p1100, 1114 Fig.16|||Musgrave Province.|c.1220-1120 Ma.|||||
39078|Pitjantjatjara Supersuite|73225|5|Briefly described|p21|||Eastern Musgrave Province.|c.1155-1136 Ma.||||Granites.|
39078|Pitjantjatjara Supersuite|73232|6|Mentioned|p5, p12-14|Stenian|Ectasian|Musgrave Province. [Emplaced] during the Musgravian Orogeny. Deeply weathered, gradational boundary with overlying palaeovalley infill sediments in drillholes DH1a and S22i.|c. 1220-1120 Ma|||Intrudes Birksgate Complex. Intruded by Giles Complex including Alcurra Dolerite.|Includes granitic plutons.|
39078|Pitjantjatjara Supersuite|73234|6|Mentioned|p19|Stenian|Ectasian|Musgrave Province.|1220-1140 Ma||||Includes granites.|
39078|Pitjantjatjara Supersuite|73338|6|Mentioned|piii, p7|Stenian|Ectasian|Widespread throughout the Musgrave Province. Broadly coincident with the Musgrave Orogeny. Ages are of magmatic crystallisation. Dominant interval emplaced from 1180 Ma to 1140 Ma (Close 2013).|Ranges from 1220 Ma to 1120 Ma.|||||
39078|Pitjantjatjara Supersuite|73346|6|Mentioned|p2, p5-6, p24, p26|Stenian|Ectasian|Musgrave Province; dominates the province in outcrop. Produced during the 1219-1149 Ma Musgrave Orogeny.|1219-1149 Ma||||Includes granite.|
39078|Pitjantjatjara Supersuite|73437|5|Briefly described|p151, p153|Mesoproterozoic|Mesoproterozoic|Musgrave Province. Emplaced during Musgrave Orogeny as voluminous mantle-derived granitic magmas.|1220-1150 Ma||||Metagranite and orthogneiss.|
39078|Pitjantjatjara Supersuite|74367|6|Mentioned|p23|||Musgrave Province.||||||
37091|Plumbago Formation|60485|2|Defined|p26-27, p28 Fig. 2|Statherian|Statherian|Important marker unit in Willyama Supergroup evolution. Overlies Bimba Fm. and Ettlewood Calc-Silicate Mbr (Allendale Metasediments). Grades upwards into Strathearn and Mount Howden Groups. Age: 1693+/-3Ma.  Max. thickness: ~30m.  Type section included.||||||03-MAR-05
37091|Plumbago Formation|61736|4|Described|p664, p666 Fig. 3|Paleoproterozoic|Paleoproterozoic|Basal unit of the Strathearn Group (lower section). Overlies the Bimba Formation. Age: 1695+/-3Ma (max. depositional age), 1693+/-3Ma. Geological province: Olary Domain. See also p667-8.||||||24-FEB-10
37091|Plumbago Formation|62535|4|Described|p663-674|Paleoproterozoic|Paleoproterozoic|Olary Domain. A regionally-extensive, thin (1-30m thick) horizon. SHRIMP U-Pb zircon age of protolith: probably close to age of deposition. Several other (similar) ages given.|1695 +/- 3 Ma (maximum depositional age).|Basal Saltbush Subgroup.||Overlies Bimba Formation. Is overlain by Walparuta Formation or Mount Howden Subgroup. Correlated with Ettlewood Calc-Silicate Member.|Graphitic, laminated metasiltstone.|
37091|Plumbago Formation|62592|5|Briefly described|p14, p16 Fig.2.2.|Statherian|Statherian|Olary Domain, Curnamona Province. There is a hiatus of c.40 m.y. between deposition of this unit and the Mount Howden Subgroup.|1693 +/- 3 Ma.|Basal unit in Strathearn Group.||||
37091|Plumbago Formation|62641|6|Mentioned|p286.||||1692 +/- 3 Ma (Page et al.,2003).|Top of Willyama Supergroup.||||
37091|Plumbago Formation|62993|5|Briefly described|p3, p13, 14,15, 37|Paleoproterozoic|Paleoproterozoic|Olary Domain. A thin volcaniclastic unit of great significance, directly overlying and forming a lithostratigraphic couplet with the base metal anomalous Bimba Formation.||Larry Macs Subgroup||Overlies Bimba Formation. Overlain by Raven Hill Formation, Walparuta Formation, Alconie Formation.|Fine grained, platy, graphititc psammitic volcaniclastic schists.|17-DEC-21
37091|Plumbago Formation|63102|4|Described|p13-15,20,24,26,32-34,36-37,38,40,44,53|Statherian|Statherian|Geological province: Olary and Broken Hill domains, Curnamona Province. Thickess: 5-40m. Extensive, deep basin floor, thin tuffaceous unit deposited during a depositional hiatus; possibly synchronous with the Prize-Gun Supersequence boundary. Has a U-Pb zircon age of 1693+\-3 Ma from a sample of fine-grained tuffaceous metasandstone (Page et al. 1998, 2000, Page et al. in prep.), as well as identical ages from samples in Olary and Broken Hill domains. Volcaniclastic sheet that chronostratigraphically ties the Olary and Broken Hill domains, and forms a regional couplet with the underlying Bimba Formation/Ettlewood Calc-silicate Member. Considered to be one of two possible markers beds separating the Curnamona and Strathearn groups. This unit has a friable lithology and is poorly exposed.|1693+\-3 Ma (Page et al. in prep)|Unit of Saltbush Subgroup.||Overlain by Broken Hill Group or Mount Howden Subgroup or Oonatra Creek Formation or Walparuta Formation. Underlain by Bimba Formation.|Fine-grained psammopelite; biotite-quartz feldspar, but with minor graphite and accessory zircon.|22-OCT-19
37091|Plumbago Formation|63866|5|Briefly described|p41|||Olary Domain, Curnamona Province.|1693 +/- 4 Ma|Saltbush Group||Overlies the Bimba Formation. Equivalent to the Ettlewood Calc-Silicate Member. Overlain(possibly unconformably) by the Raven Hill Subgroup.|Tuffaceous bioite psammite.|
37091|Plumbago Formation|64741|5|Briefly described|p301 Fig. 4, p307|Paleoproterozoic|Paleoproterozoic|Of Larry Macs Subgroup (Saltbush Group). Overlies Bimba Formation. Age: 1693+/-3Ma. Geological province: Olary Domain. Interpreted to represent an ash fall punctuating a period of sediment starvation with accumulated organic matter.||||||07-FEB-11
37091|Plumbago Formation|64742|6|Mentioned|p321 Fig.3, P323.||||1693 Ma.|Unit in Saltbush Subgroup.|||Quartz-muscovite schist.|29-MAR-12
37091|Plumbago Formation|64944|4|Described|p26, p28 Fig. 1|Paleoproterozoic|Paleoproterozoic|A chronstratigraphic marker in the Olary Domain which relates to a lithologically similar metasiltstone, Allendale Metasediments, overlying and/or interbedded with the Ettlewood Calc-Silicate Member (Allendale Metasediments) in western Broken Hill Domain.||||||07-FEB-11
37091|Plumbago Formation|66302|5|Briefly described|p36 Fig.9, p37, p38, p39|Statherian|Statherian|Olary Domain, Curnamona Province. Ages are derived from Page et al. (1998, 2000 and 2005).|1693 +/- 3 Ma |Larry Macs Subgroup||Overlies the Bimba Formation.|Tuffaceous metasandstone.|
37091|Plumbago Formation|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Olary Domain.|1693 +/- 3 Ma.|Saltbush Group.||||
37091|Plumbago Formation|68126|6|Mentioned|p30||||1693 +/- 3 Ma (Page et al. in prep).|||||
37091|Plumbago Formation|70405|4|Described|P1,p9 table 1, p28, p43 Table 3|Paleoproterozoic|Paleoproterozoic|Contain 1700 Ma detrital zircons|1693 Ma - 1700 Ma|Larry Macs Subgroup||Overlies Bimba formation|Volcaniclastic sediments, immature, fine grained psammite and metasiltstone, locally graphitic.|
37091|Plumbago Formation|70657|4|Described|p10 Fig.4, p13 Fig.6, p14-17, p20, p24|Statherian|Statherian|See also p33-34, p36-46, p58. Conor (2000, 2004). Curnamona Province; Olary, Broken Hill Domains. An important regional marker unit (significance elaborated), overlain by several major stratigraphic units. 5-40m thick. Generally not mineralised (exceptions include the Dome Rock Mine). Equivalent to upper part of Ettlewood Calc-Silicate Member (Allendale Metasediments).|1693 +/- 3 Ma (Page et al., 2005).|Larry Macs Subgroup||Overlies Bimba Formation. Underlies Black Maria Formation (Raven Hill Subgroup), Walparuta Formation, Alconie Formation (Strathearn Group) gradationally.|Medium- to dark-grey, planar-bedded, fine-grained, graphitic micaceous psammite, distinctly volcaniclastic. Friable, poorly exposed.|
37091|Plumbago Formation|70658|5|Briefly described|p2-3, 5, 7, 15-16, 19, 25, 29, 47|Paleoproterozoic|Paleoproterozoic|Olary Domain, Curnamona Province. Type section on east Ameroo Hill saddle. Is overlain locally by various units of widely-differing ages (listed).|1693 Ma.|Larry Macs Subgroup.||Overlies Bimba Formation.|Graphitic tuffaceous psammite. Volcaniclastics. Basal augen-textured quartzo-feldspathic tuff. Mainly dark grey, thinly graded-bedded psammite.|
37091|Plumbago Formation|70829|6|Mentioned|p33|||Curnamona Province. Known to contain graphite which may contribute to the high conductivity of Olary Domain lithosphere.||||||
37091|Plumbago Formation|72461|6|Mentioned|p6||||1693 +/- 3 Ma|||||
37091|Plumbago Formation|73021|6|Mentioned|p224|||||Broken Hill Group.||||
37091|Plumbago Formation|73429|5|Briefly described|p106 Fig.2|Statherian|Statherian|Curnamona Province, Olary Domain||Larry Macs Subgroup||Overlies Bimba Formation, underlies Raven Hill Subgroup||
24460|Point Ellen Formation|38699|2|Defined|p28|early Pleistocene|early Pleistocene|See also p16.||||||23-JUN-08
24460|Point Ellen Formation|38700|4|Described|p38|||||||||
24460|Point Ellen Formation|39522|6|Mentioned|p86|||||||||
24460|Point Ellen Formation|39524|6|Mentioned|p72|||||||||
24460|Point Ellen Formation|39835|6|Mentioned|p284|||||||||
24460|Point Ellen Formation|40643|6|Mentioned|Table 1|||||||||
24460|Point Ellen Formation|44133|5|Briefly described|p66, 222|Early Pleistocene|Early Pleistocene|Overlies Cape Jervis Formation.||||||23-JUN-08
24460|Point Ellen Formation|60958|5|Briefly described|Map Legend|Pleistocene|Pleistocene|Pinkish grey fossiliferous fine-grained laminated calcarenite or silty limestone and shelly sandstone. Geological Province: Saint Vincent Basin.||||||
24460|Point Ellen Formation|61121|5|Briefly described|Map legend|Pleistocene|Pleistocene|Pinkish grey fossiliferous, fine-grained laminated calcarenite or silty limestone and shelly sandstone. Age: ~1.2Ma (Strontium isotope). Geological  Province: St. Vincent Basin.||||||07-JUN-05
24460|Point Ellen Formation|61155|5|Briefly described|p17|Pleistocene|Pleistocene|Overlain by Glanville Formation. Age: <1.5Ma. Geological Province: St Vincent Basin. Point is Pt in text of chart.||||||
24460|Point Ellen Formation|64282|5|Briefly described|Map legend|Pleistocene|Pleistocene|Geological Province: St Vincent and Eucla Basins.  Age: ~1.2Ma. Pinkish grey, fossiliferous, fine-grained, laminated calcarenite or silty limestone and shelly sandstone with Brachidontes. Elphidum, Quinqueloculina and Balillaria remains.||||||24-JUL-08
24460|Point Ellen Formation|65375|5|Briefly described|p7, pp38-39.|Pleistocene|Pleistocene|Equivalent to Burnham Limestone. 51 faunal species described; 36 still living, 15 from Early Pleistocene.|c.1.2 Ma.||||Thin, sandy to silty fossiliferous limestone.|
24460|Point Ellen Formation|65921|5|Briefly described|p1, p2 (map legend).|Quaternary|Quaternary|Occurs as low cliffs at Point Ellen (Vivonne Bay). Episodes of high sea level are marked by the fossil-bearing sediments of this Formation.|||||Calcarenite and cobble conglomerate with a prominent mollusc fossil fauna.|
24460|Point Ellen Formation|67462|5|Briefly described|Map legend.|Pliocene|Pliocene|Western Saint Vincent Basin.||||Overlies Hallett Cove Sandstone.||
24460|Point Ellen Formation|68131|6|Mentioned|p7, p17|Pleistocene|Pleistocene|Yorke Peninsula.||||||
24460|Point Ellen Formation|68715|6|Mentioned|p31 Fig.5|Pliocene|Pliocene|St Vincent Basin. Early Pliocene age.||||||
24460|Point Ellen Formation|69372|5|Briefly described|p25 Fig.2|||Overlies Cape Jervis Formation at that unit's type section at Cape Jervis.||||Overlies Cape Jervis Formation.|Limestone. Is overlain by calcrete.|
24460|Point Ellen Formation|73107|5|Briefly described|Map legend.|Pleistocene|Pleistocene|Fossils include Brachidontes, Elphidium, Quinqueloculina, and Batillaria remains.|~1.2 Ma (Sr isotope).||||Pinkish grey fossiliferous fine-grained laminated calcarenite or silty limestone and shelly sandstone.|
77225|Point James Granite|66519|2|Defined|p31-34.|Mesoproterozoic|Mesoproterozoic|A small, ~5 km wide circular pluton; no significant post-intrusion deformation. Type locality on wavecut platform at Point James. |1580 +/- 15 Ma (Payne 2008). SHRIMP U-Pb|Unit in Munjeela Suite.||Sharp intrusive contacts with granite of the St Peter Suite.|Quartz-K-feldspar-plagioclase-muscovite-biotite +/- garnet granite; intermingled leucocratic (biotite-absent) phases. Dominantly coarse-grained equigranular leucogranite. Rapakivi texture common.|05-FEB-14
77225|Point James Granite|71317|5|Briefly described|p175|||Contains xenoliths dated at 1639 +/- 29 Ma.|c. 1590-1575 Ma|||||
77226|Point Sinclair Granite|66519|2|Defined|p31, pp33-34.|Mesoproterozoic|Mesoproterozoic|Type locality at Point Sinclair, where it forms a high, rounded headland. Occurs as low wavecut platforms at Point Bell. Forms an elongate pluton. At Point Bell, multiple intrusive phases are present, deformed by syn- and post-intrusion shear zones. Dating: SHRIMP U-Pb zircon.|1591 +/- 11 Ma; 1577 +/- 9 Ma (Payne 2008).|Unit in Munjeela Suite.|||Medium- to coarse-grained quartz-K-feldspar-plagioclase-muscovite-biotite-garnet granite; minor less peraluminous phases; metasedimentary enclaves common locally.|15-OCT-12
27881|Polly Conglomerate|22650|6|Mentioned|p 166|Devonian|Devonian|Of the Finke Group..||||||23-NOV-06
27881|Polly Conglomerate|22760|6|Mentioned|p340|||Of the Finke Group.||||||23-NOV-06
27881|Polly Conglomerate|22826|6|Mentioned|p576|Devonian|Devonian|||||||
27881|Polly Conglomerate|23858|5|Briefly described|p916|||Of Finke Group. Overlain by Langra Conglomerate. Geological Province: Amadeus Basin.||||||23-NOV-06
27881|Polly Conglomerate|30544|6|Mentioned|p51|||On map legend||||||
27881|Polly Conglomerate|31566|6|Mentioned|p244|||Devonian||||||
27881|Polly Conglomerate|31567|3|Fully described|p276|||||||||
27881|Polly Conglomerate|33832|6|Mentioned|p8|||Stratigraphy||||||
27881|Polly Conglomerate|33844|6|Mentioned|Table 1|||||||||
27881|Polly Conglomerate|33971|3|Fully described|p28|||Of the Finke Group.||||||23-NOV-06
27881|Polly Conglomerate|34580|4|Described|Table 1|||Devonian - Carboniferous||||||
27881|Polly Conglomerate|35102|6|Mentioned|Fig.17|||||||||
27881|Polly Conglomerate|43035|6|Mentioned|p23|||Of the Finke Group.||||||23-NOV-06
27881|Polly Conglomerate|44133|5|Briefly described|p44|Carboniferous?|Late Devonian|Of the Finke Group. Conformably overlies Mereenie Sandstone. Geological Province: Pedirka Basin.||||||
27881|Polly Conglomerate|44323|14|Not recorded|map legend|Carboniferous|Devonian|SG53-6. Dev-Carb. Of the Finke Group.||||||23-NOV-06
27881|Polly Conglomerate|44342|4|Described|p.7, Table 2|Carboniferous|Devonian|SG/53-5. Dev-Carbon.||||||
27881|Polly Conglomerate|44343|14|Not recorded|map legend|Carboniferous|Devonian|Devonian-Carbon.||||||
27881|Polly Conglomerate|44393|4|Described|p.3,7,8,Tb.1,Fig.1|Carboniferous|Devonian|Correlated with Pertnjara Group. Dev-Carb.||||||
27881|Polly Conglomerate|45041|4|Described|p104|||Devonian. Of the Finke Group.||||||23-NOV-06
27881|Polly Conglomerate|48865|2|Defined|p.3,4,Fig.29|Carboniferous|Devonian|Overlain by Langra Formation.||||||23-NOV-06
27881|Polly Conglomerate|48890|4|Described|p.51|Carboniferous|Devonian|See also Tb.2,Tb.3,Fig.4. Of the Finke Group.  Devonian to Carboniferous. Defn on Tech.File G/53-6.||||||23-NOV-06
27881|Polly Conglomerate|50372|5|Briefly described|Map Legend|Devonian|Devonian|Of Finke Group. Geological Province: Amadeus Basin. Well rounded pebble to cobble, rarely boulder conglomerate in a clayey sand matrix. Clasts predominantly composed of granite, gneiss and quartzite.||||||
27881|Polly Conglomerate|65233|5|Briefly described|p13|Devonian|Devonian|Of the Finke Group. Overlain by Horsebend Shale.||||||07-FEB-11
27881|Polly Conglomerate|65309|4|Described|p6 Table 1, pp13-14, p19.|Devonian|Devonian|Sits directly on basement rock from which it is derived, and occurrence is restricted to immediately north of exposed basement. Maximum outcrop thickness is 65m. Type area at Horseshoe Bend, where clasts include material from Winnall beds. |Deposition age c.380 Ma.|Unit in Finke Group.|||Well-rounded pebble to cobble, rarely boulder conglomerate; white medium to coarse clayey sand matrix; clasts predominantly composed of granite, gneiss and quartzite.|
27881|Polly Conglomerate|65342|6|Mentioned|p10.|||Pedirka Basin. Max. thickness at least 393 m.||||Overlies Mereenie Sandstone. Is overlain by Langra Sandstone.||
27881|Polly Conglomerate|65489|6|Mentioned|p63|||Amadeus Basin. Contains potential reservoir beds.||||||
27881|Polly Conglomerate|69438|3|Fully described|p23:2-3, 20, 40-41|Late Devonian|Late Devonian|Wells et al. (1966). Amadeus Basin. Type locality is on the N flank of the Black Hill Range where it is 40m thick; up to 393m thick elsewhere, and locally absent from the Group's succession. Alluvial fan or proximal braided stream deposit.||Finke Group.||Unconformably overlies Winnall and Inindia beds and Stairway Sandstone. Is overlain conformably and gradationally by Langra Formation.|Polymictic, clast- to matrix-supported conglomerate, with interbeds of medium- to coarse-grained sandstone and rare brown or green siltstone.|12-JUL-16
27881|Polly Conglomerate|69449|5|Briefly described|p34:5|Devonian|Devonian|||Finke Group.||Overlies Mereenie Sandstone. Is overlain by Langra Formation.||12-JUL-16
27881|Polly Conglomerate|69673|6|Mentioned|p64 fig 53, p149|||||Finke Group||Overlain by Langra Formation||
27881|Polly Conglomerate|71279|5|Briefly described|p355 Fig.2|Late Devonian|Late Devonian|Amadeus Basin.||Finke Group.||||
27881|Polly Conglomerate|72476|5|Briefly described|p36|Silurian|Silurian|Amadeus Basin. Time-temperature thermal history diagram.|||||Coarse conglomerate.|
27881|Polly Conglomerate|73085|6|Mentioned|p1|late Devonian|late Devonian|||Finke Group||Overlain by Langra Formation. Equivalent to Parke Siltstone (Pertnjara Group).||
27881|Polly Conglomerate|73281|6|Mentioned|Appendix (DIP)|||See DIP034_Petroleumdata.xlsx and DIP034_Welldata.xlsx.||||||
36780|Pondanna Dacite Member|24346|4|Described|p103, p105|||New member of Yardea Dacite. Includes some rocks previously mapped as "Eucarro Dacite". Formerly referred to as 'black dacite" of Yardea Dacite. Overlain by Moonaree Dacite Member.||||||
36780|Pondanna Dacite Member|70659|6|Mentioned|p6 fig 2|Mesoproterozoic|Mesoproterozoic|||Yardea Dacite||||
36780|Pondanna Dacite Member|70816|5|Briefly described|p4-5|||Gawler Ranges region.||Unit of Yardea Dacite||Overlain by Moonaree Dacite Member.|Amygdalar, vesicular facies, includes granitic and lithic clasts.|
36780|Pondanna Dacite Member|71317|4|Described|p1, p20, p54, p57-p58, p68-p69|Mesoproterozoic|Mesoproterozoic|Originally mapped as the Yardea Dacite before being seperated out by Allen et al., 2003. Referred to as the Pondanna Dacite on p57 and p58. Outcrop extent of 150km by 50km. Dips shallowly to the north and outcrop is dominated by red-brown dacite. Intersected in MSDP05 (drillhole 288771), MSDP06 (drillhole 288772) and MSDP07 (drillhole 288773). Lithology and detailed outcrop characteristics are provided. An estimated thickness of at least 250m is given. See also p75, p84-p88, p90-p94, p96-p99, p103-p104, p113-p114, p143, p150, p156, p165-p166, p168-p170, p172-p173, p176.||Yardea Dacite||Overlies the Eucarro Rhyolite. Overlain by the Moonaree Dacite Member,Yartoo volcaniclastics and the Immarna Group.|Black, sparsely porphyritic quenched flow base, red-brown, porphyritic flow center with spherulitic to granophyric groundmass and prominent columnar jointing with a preserved vesicular flow top.|
36780|Pondanna Dacite Member|71418|6|Mentioned|p21|Mesoproterozoic|Mesoproterozoic|Geological province: Gawler Craton.||||||
36780|Pondanna Dacite Member|71559|4|Described|p16, p19-22|Mesoproterozoic|Mesoproterozoic|Geological province: Gawler Craton.||Unit of Yardea Dacite.||Overlain by Yartoo Volcaniclastics.|Dacite, massive, red, commonly colmnar jointed; porphyritic with phenocrysts of plagioclase and pyroxene in a fine-grained spherulitic to granophyric groundmass.|19-JUN-19
36780|Pondanna Dacite Member|71560|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|||Yardea Dacite.|||Dacite, massive, red, commonly columnar-jointed; porphyritic with phenocrysts of plagioclase and pyroxene in a fine-grained spherulitic to granophyric groundmass.|
36780|Pondanna Dacite Member|72065|4|Described|p105-110,112-116,119|Calymmian|Calymmian|Geological province: Gawler Craton. Also referred to as Pondanna Dacite in text. Dimensions: ~160km E-W and ~10-60km N-S, 250m thick and >1000km3. Lavas type: Peraluminous, ferroan to marginal magnesian. Emplaced in >1My from around 1588 Ma (Jagodzinski et al., 2016). Comprises three textural facies: black or grey (no or lacking feldspar and pyroxene alteration) base, massive red (displays feldspar and pyroxene alteration) interior, and vesicular margins. See major- and trace-element composition plots on p108 Fig 5. Contains 'GRV-type' crystal clusters: pyroxene and Fe-Ti oxides+\-apatite+\-zircon+\-plagioclase. Crystal formation likely formed from an intermediate evolved phase (after Moonaree Dacite crystal formation, and before Eucarro Rhyolite crystal formation) of the Upper GRV parental melt (likely hot, dry, and relatively reduced, as pyroxenes predominate over biotite). Interpreted that crystals formed within the magmatic system, and required a subsequent event or rejuvenation (magma recharge: increased temperature or melt volatile content for example) to free the crystal clusters prior to, and during extrusive unit emplacement.||Unit of Yardea Dacite.||Underlain by Eucarro Rhyolite.||
36780|Pondanna Dacite Member|72089|5|Briefly described|p2|||Gawler Craton.  Rapidly erupted.||Yardea Dacite|||Dacitic lava.|
36780|Pondanna Dacite Member|72090|4|Described|p12, p50, p52-p53|||Gawler Craton. Intersected by MSDP06 drillhole. Flow banding was measured in multiple drillholes. See also p55-p56, p59, p100, p110.||Yardea Dacite, Gawler Range Volcanics, Upper||Overlies the Eucarro Rhyolite.|Dark grey to moderate reddish brown, porphyritic, unweathered to highly weathered dacite.|
36780|Pondanna Dacite Member|72462|5|Briefly described|p8|||Flow has a finer-grained and less crystal-rich black flow-banded quenched base and purple-brown central portion with a mingled to gradational boundary. Colour and textural differences are the result of differential cooling rates.||Yardea Dacite, Gawler Range Volcanics|||Red-brown porphyritic dacite, composed of plagioclase, potassium feldspar, altered ferromagnesian phases, and very rare quartz.|
36780|Pondanna Dacite Member|72464|6|Mentioned|p2|Mesoproterozoic|Mesoproterozoic|Gawler Craton.||||||
36780|Pondanna Dacite Member|73110|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic||||||Dacite, massive, red, commonly columnar jointed; porphyritic with phenocrysts of plagioclase, pyroxene.|
72788|Pondrinie Basalt|62537|6|Mentioned|p191 Fig.2. |Middle Cambrian|Middle Cambrian|Warburton Basin.||||Intrudes Dullingari group.||
72788|Pondrinie Basalt|63056|5|Briefly described|p81 Fig. 2|Late Cambrian|Middle Cambrian|Thickness: 30m. Geological Province: Warburton Basin. Extrusive basalt.||||||07-FEB-08
72788|Pondrinie Basalt|65489|5|Briefly described|p96, p120|Early Ordovician|Early Ordovician|Eastern Warburton Basin. Extrusive.||||Intercalated with Innamincka Formation.||
72788|Pondrinie Basalt|67536|6|Mentioned|Map Legend|||Warburton Basin.|||||Trachytic basalt, some with olivine, some amygdaloidal.|
72788|Pondrinie Basalt|68731|6|Mentioned|p170 Fig 3.83|Late Ordovician|Early Ordovician||||||Comprises extrusive basalt.|
72788|Pondrinie Basalt|69982|3|Fully described|p17-19,p40-42,p45,p95,p104,p159,p224|Middle Ordovician|Early Ordovician|New name. Occurs in the interval 2367.4 - 2397.6 m in the type well, Pondrinie 5. Warburton Basin. Up to 30 m thick. Probably extrusive. Brief thin section descriptions. Composite log shown. Details of wells with hydrocarbon shows.||||Is interbedded with Innamincka Formation.|Thin beds of olivine basalt; also trachytic basalt and acid tuff.|
35621|Ponto Group|24345|5|Briefly described|p85|Cambrian|Cambrian|Geological Province:  Wonominta Block.||||||
35621|Ponto Group|24599|5|Briefly described|p494 Fig. 2|Cambrian|Cambrian|Metasediments and volcanics.||||||
35621|Ponto Group|50618|5|Briefly described|p248|Middle Cambrian|Early Cambrian|Of Stevens et al (2000). Upgrading of Ponto beds?? Geological Province: Wonominta Block.||||||
35621|Ponto Group|63789|5|Briefly described|Map Legend|Ordovician|Late Cambrian|Includes Baroorangee Creek Subgroup. In the Koonenberry Fault area.||||||27-NOV-08
35621|Ponto Group|63793|4|Described|p18, p22, p34-38, p76-77.|||Stevens et al. (2000). Formerly part of Wonominta beds (Warris 1967), Ponto beds (Mills 1992). High grade metamorphic rocks, multiply deformed; no primary textures preserved.  Unfossiliferous. White quartz veins abundant. Hosts Grasmere copper mine. Much of outcrop area has not been prospected.|||Includes Baroorangee Creek Subgroup.|Faulted against Kara beds. Is unconformably overlain by Ravendale Formation.|Phyllites and fine-grained mica-schists, with lesser tholeiitic pillow lavas and tuffs, thinly laminated quartzofeldspathic tuffs and weakly calcareous and dolomitic pelites.|19-JAN-15
35621|Ponto Group|64169|5|Briefly described|p18, p19|||Supersedes Ponto beds. Subdivided into: Nutherangie, Palgamurtie and Baroorangee Creek Subgroups. Geol. prov: Mount Daubeny Basin/Koonenberry Belt. In western half of GRASMERE sheet - atypical rocks characterise Baroorangee Creek Subgroup.||||||14-MAY-08
35621|Ponto Group|64671|5|Briefly described|Map legend|||Tentatively subdivided into Barroorangee Creek, Palgamurtie and Noonthorangee Subgroups. Thick dark grey and maroon phyllite units interbedded with well-indurated fine-gr. turbiditic quartzofeldspathic arenites. Massive to well-cleaved tholeiitic metabasalt...||||||07-MAY-13
35621|Ponto Group|64680|5|Briefly described|Map Legend|Ordovician|Middle Cambrian|Includes Noonthorangee, Palgamurtie, and Baroorangee Creek Subgroups. Thick dark grey and maroon phyllite units interbedded with well-indurated fine-grained turbiditic quartzofeldspathic arenites. Massive to well-cleaved tholeiitic metabasalts.||||||
35621|Ponto Group|64682|5|Briefly described|Map Legend|Ordovician|Late Cambrian|Includes Noonthorangee Subgroup. Thick dark grey and maroon phyllite units interbedded with well-indurated fine-grained turditic quartzofeldspathic arenites. Massive to well-cleaved tholeiitic metabasalts, and laminated siliceous tuffs.||||||
35621|Ponto Group|64684|5|Briefly described|Map Legend|Ordovician|Late Cambrian|Includes Palgamurtie Subgroup.||||||
35621|Ponto Group|64686|5|Briefly described|Map Legend|Ordovician|Middle Cambrian|Includes Palgamurtie and Barooangee Creek Subgroups. Thick dark grey and maroon phyllite units interbedded with well-indurated fine-grained turbiditic quartzofeldspathic arenites. Massive to well-cleaved tholeiitic metabasalts, + laminated siliceous tuffs||||||
35621|Ponto Group|64687|5|Briefly described|Map Legend|||||||||
35621|Ponto Group|65381|5|Briefly described|p689, 691, Fig 2|Middle Cambrian|Early Cambrian|Of the Wertago zone, Broken Hill; distal turbidites with minor tholeiitic volcanics.||||||07-MAR-12
35621|Ponto Group|66623|1|Redefined|p10, p57, pp74-97. |Cambrian|Cambrian|Formerly part of Wonominta beds (Warris 1967); named the Ponto beds (Mills 1972); renamed Ponto Group (Stevens et al. 2000); redefined this study. Fault-bounded, highly-deformed rocks, c.5.5 km thick. No fossils found. Characteristically forms low relief rises. Similar calc-alkaline chemistry as the coeval lower Gnalta Group. Equivalent age and geochemistry to the Kars Zone in the Loch Lillly - Kars Belt. Bittles Tank Volcanics correlated with Glenelg Complex of Victoria's Stavely Belt. Hosts several small copper deposits. Geophysical properties described.|Tuffs aged 512-509 Ma (Black 2005). ||Includes Baroorangee Creek, Weinteriga Creek, Grasmere, Cannela, Noonthorangee, Koonenberry, Yandenberry Formations and Bittles Tank Volcanics.|Is unconformably overlain by Mutawintji Group and the Mount Daubeny Formation.|Predominant fine-grained distal sequence of metamorphosed mudstone, siltstone and sandstone; minor tholeiitic pillow lavas and sills, exhalative (quartz-magnetite rocks) units, and felsic air-fall tuffs.|
35621|Ponto Group|66917|5|Briefly described|Map legend|Cambrian|Cambrian|Does not crop out in the map area.|||||Dark grey to maroon phyllite interbedded with fining-upward quartzo-feldspathic psammites; originally interbedded siltstone and minor sandstone; regionally metamorphosed to greenschist facies.|
35621|Ponto Group|66918|5|Briefly described|Map legend|Cambrian|Cambrian||||Includes Baroorangee Creek Formation, Bittles Tank Volcanics and Grasmere Formation.||Dark grey to maroon phyllite interbedded with fining-upward quartzo-feldspathic psammites; originally interbedded siltstone and minor sandstone; regionally metamorphosed to greenschist facies.|
35621|Ponto Group|66922|5|Briefly described|Map legend|Cambrian|Cambrian||||Includes Cannela Formation.||Dark grey to maroon phyllite interbedded with fining-upward quartzo-feldspathic psammites; originally interbedded siltstone and minor sandstone; regionally metamorphosed to greenschist facies.|
35621|Ponto Group|66927|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
35621|Ponto Group|66929|5|Briefly described|Map legend|||Variable strong to weak magnetic signature. Unfossiliferous.|||Includes Baroorangee Creek, Palgamurtie and Noonthorangee Subgroups.||Thick dark grey and maroon phyllite units interbedded with well-indurated, fine-grained turbiditic quartzofeldspathic arenites; massive to well-cleaved tholeiitic metabasalts and laminated siliceous tuffs.|
35621|Ponto Group|66933|5|Briefly described|Map legend|Ordovician|Middle Cambrian|Variable strong to weak magnetic signature.|||Includes Noonthorangee and Palgamurtie Subgroups.||Thick dark grey and maroon phyllite units interbedded with well-indurated fine-grained turbiditic quartzofeldspathic arenites; massive to well-cleaved tholeiitic metabasalts and laminated siliceous tuffs.|
35621|Ponto Group|67105|5|Briefly described|p650-651, 653-654, 658-659, 661-663|Cambrian|Cambrian|See also p665-666. East of the Gnalta Group, Koonenberry Belt. Deep-water environment; fore-arc sequence. Tectonic settings discussed. Upper greenschist to amphibolite (muscovite-biotite schist) grade. Strongly deformed.|511.7 +/- 3.5 Ma (SHRIMP II zircon: Black, 2005).||Bittles Tank Volcanics.||Deep-marine sedimentary package (mudstone and siltstone) with tholeiitic lavas and extensive laminated cherty felsic tuffs. Includes magnetic phyllite with intercalated calc-silicate horizons.|
35621|Ponto Group|67107|6|Mentioned|p697, 701|||Mentioned in a graph of Pb isotope data for the Lachlan Orogen.|||Bittles Tank Formation.||Includes metamorphosed marine clastic rocks with mafic dykes and flows of fundamentally tholeiitic composition.|
35621|Ponto Group|67207|5|Briefly described|Map legend.|Cambrian|||||Includes Cannela Formation.|Map key shows: overlies Teltawongee Group, is overlain by Warratta Group[?].|Dark grey to maroon phyllite interbedded with fining-upward quartzo-feldspathic metasandstone; originally interbedded siltstone and minor sandstone; regionally metamorphosed to greenschist facies.|25-SEP-13
35621|Ponto Group|67208|5|Briefly described|Map legend.|Cambrian|Cambrian||||Includes Bittles Tank Volcanics and Yandenberry Formation.||Dark grey to maroon phyllite interbedded with fining-upward quartzo-feldspathic metasandstone; originally interbedded siltstone and minor sandstone; regionally metamorphosed to greenschist facies.|
35621|Ponto Group|67322|4|Described|p3 Fig.1, p11, p39; Fig. 5|Late Cambrian|Middle Cambrian|Koonenberry Belt, Delamerian Orogen. Of Mills (in Greenfield et al., 2010). At least 5500 m thick. Unfossiliferous. Age from tuffs in Noonthorangee Formation - not well constrained. Occurs in the Kayrunnera-Koonenberry region.|||Weinteriga Creek, Grasmere, Noonthorangee, Koonenberry, Yandenberry, Cannela and Baroorangee Creek Formations; Bittles Tank Volcanics.|Intruded by the Bittles Tank Volcanics.|Variably metamorphosed, fine-grained marine clastic rocks (phyllites, schists, fine-grained sandstones and mudstones). In the middle are extrusive rocks, including enriched MORB tholeiitic pillow lavas, basaltic flows and basic tuffs.|22-FEB-18
35621|Ponto Group|68822|6|Mentioned|p330|||Contains c 510 Ma tuff bands.||||||
35621|Ponto Group|69001|6|Mentioned|p2 Fig.1B|Cambrian|Cambrian||||Includes the Cannela Formation.|||
35621|Ponto Group|69043|5|Briefly described|p4, p100, p104|||Fore-arc eruptive deposits from the subduction-related Mount Wright volcanic arc; coeval with Cymbric Vale Formation to the W. Other similar age determinations given.|511.7 +/- 3.5 Ma (Black, 2005).|||||
35621|Ponto Group|69961|5|Briefly described|Map legend|Cambrian|Cambrian||||Includes Noonthorangee, Koonenberry and Yandenberry Formations and Bittles Tank Volcanics.||Undifferentiated: dark grey to maroon phyllite interbedded with fining-upward quartzo-feldspathic metasandstone; originally interbedded siltstone and minor sandstone; regionally metamorphosed to greenschist facies.|
35621|Ponto Group|70013|5|Briefly described|Map legend|Middle Cambrian|Early Cambrian|In the Koonenberry Belt, quartzofeldspathic sandstone, metabasalt, trachyandesite and dacitic tuff are intercalated. Crops out in N part of the Kars Zone. Interpreted equivalent to sedimentary and volcanic rocks in the Wirryilka, Loch Lilly and Kars (geophysical basement) Zones.|||||Thickly bedded dark grey phyllite units.|
35621|Ponto Group|70037|6|Mentioned|p11|||||||||
35621|Ponto Group|70210|5|Briefly described|p1, p38|Middle Cambrian|Middle Cambrian|Koonenberry-Tibooburra district. Four felsic tuffs from this unit and Cymbric Vale Formation have indistinguishable SHRIMP ages of c.511 Ma.|||Canella Beds.|||
35621|Ponto Group|70296|6|Mentioned|p1-2, p19-21, p24|||Koonenberry District. Four samples dated. Three are felsic tuffs. SHRIMP ages include 511.4 +/- 3.7 Ma; 509.4 +/- 3.4 Ma; 512.8 +/- 3.3 Ma and 497.5 +/- 3.3 Ma for a felsic tuff or volcanic flow. Dated tuffs correlated with dated tuff in Cymbric Vale Formation, suggesting both units saw the same volcanic event at ~511.1+/-1.7 Ma.|||Includes the Mount Daubeny Formation [?].|||22-JAN-21
35621|Ponto Group|70648|5|Briefly described|Map Legend|Cambrian|Cambrian||||Includes Bittles Tank Volcanics, Yandenberry Formation, Koonenberry Formation, Noonthorangee Formation.||Dark grey to maroon phyllite interbedded with upward fining quartzo-feldspathic metasandstone; originally interbedded siltstone and minor sandstone; regionally metamorphosed to greenschist facies.|20-JAN-22
35621|Ponto Group|70650|5|Briefly described|Map Legend|Cambrian|Cambrian||||Includes Bittles Tank Volcanics, Grasmere Formation, Baroorangee Creek Formation.|Intruded by diorite of Bittles Tank Formation.|Dark grey to maroon phyllite interbedded with upward fining quartzo-feldspathic metasandstone; originally interbedded siltstone and minor sandstone; regionally metamorphosed to greenschist facies.|20-JAN-22
35621|Ponto Group|70651|5|Briefly described|Map Legend|Cambrian|Cambrian||||Includes Bittles Tank Volcanics, Noonthorangee Formation, Grassmere Formation, Weinteriga Creek Formation, Baroorangee Creek Formation.||Dark-grey to maroon phyllite interbedded with upward fining quartzo-feldspathic metasandstone; originally interbedded siltstone and minor sandstone; regionally metamorphosed to greenschist facies;  mafic intrusions, and extrusive mafic lavas.|
35621|Ponto Group|70749|6|Mentioned|p43|Cambrian|Cambrian|Southern Thomson and Koonenberry area.||||||
35621|Ponto Group|70838|4|Described|p266,p268-272,p274-275,p277-278,p280-281|Cambrian|Cambrian|Koonenberry Belt. Suggested deposition in deep water at the foot of a continental slope. Texturally immature: possible tectonic settings discussed (convergent margin preferred). Coeval with Teltawongee Group. Maximum depositional age is poorly constrained. Deformed during the Delamerian Orogeny (c.500 Ma). Cut by an undeformed felsic body dated 496.3 +/- 3.1 Ma (Black, 2005). Detrital zircon analyses.|c.508 Ma (maximum deposition age).||Noonthorangee Formation, Bittles Tank Volcanics.|Faulted against Grey Range Group.|Texturally immature, finely bedded mudstones and siltstones metamorphosed at greeenschist to lower-amphibolite facies.|
35621|Ponto Group|71262|5|Briefly described|p3, p5 Fig 2,  p8 Fig 5, p9, p12|Cambrian|Cambrian||||Includes Bittles Tank Volcanics?||Includes magnetite-rich members.|
35621|Ponto Group|71415|5|Briefly described|p11,15|Cambrian|Cambrian|Geological province: SW Thomson Orogen. Of the Kooneberry Belt; of Eromanga Basin. Sedimentary sequence related to c. 510 Ma volcanics of the Mount Wright Arc. Underwent deformation and greenschist facies metamorphism during c. 500 Ma Delamarian Orogeny.||||Overlies the Grey Range Group.||19-AUG-19
35621|Ponto Group|71593|5|Briefly described|p188-p189|Early Cambrian|Early Cambrian|Koonenberry Province. Hosts Besshi-type VHMS Cu-Zn prospects in E-MORB-like mafic volcanics.|c. 511-506 Ma||||Mafic volcanics.|
35621|Ponto Group|71965|5|Briefly described|p894|Cambrian|Cambrian|Geological province: Koonenberry Belt, Delamerian Orogen. Volcanism c. 510 Ma associated with development of the Mount Wright continental magmatic arc (Greenfield et al., 2010; Greenfield et al., 2011).||||||
35621|Ponto Group|71966|6|Mentioned|p990|Cambrian|Cambrian|Geological province: Delamarian Orogen.||||||
35621|Ponto Group|72522|6|Mentioned|p131.|||Part of the basement to Mount Daubeny Basin||||Intruded by Wertago Volcanics.||
35621|Ponto Group|73093|5|Briefly described|map legend|Cambrian|Cambrian||||||Dark-grey to maroon phyllite interbedded with fining-upward quartzo-feldspathic metasandstone; regionally metamorphosed to greenschist facies.|09-DEC-21
35621|Ponto Group|73177|5|Briefly described|p1098, 1114-1115 Figs.16-17|Middle Cambrian|Early Cambrian|||Grey Range Group.|Bittles Tank Volcanics, Noonthorangee Formation.|||
35621|Ponto Group|73430|6|Mentioned|p494|Middle Cambrian|Early Cambrian|Koonenberry Belt. Deformed in Delamerian Orogeny.|||||Sedimentary unit.|
72282|Poodla Granite|62514|5|Briefly described|p747 Fig. 2, p753|Mesoproterozoic||Of the Poodla Suite.  Age: c.1629+/-12Ma (Cook et al 1994). The name Poodla Hill is used in one figure - possibly name is incorrect?||||||09-SEP-13
72282|Poodla Granite|65375|6|Mentioned|p13.|Paleoproterozoic|Paleoproterozoic||c.1630 Ma.|||||
78351|Poodla Hill Suite|62514|5|Briefly described|p748 Fig. 3|Paleoproterozoic|Paleoproterozoic|Referred to as Poodla Hill only (together with the Antro Suite) - unclear what correct name is? Contains the Poodla Granite. I-type granitoids. Age: 1.64-1.63Ga.  Geological Province: Olary Domain/Curnamona Province||||||
78351|Poodla Hill Suite|63102|6|Mentioned|p6,11|Statherian|Statherian|Geological province: Curnamona Province.|~1630 Ma|||||22-OCT-19
78351|Poodla Hill Suite|67536|5|Briefly described|Map Legend|Statherian|Statherian|Curnamona Province.|ca. 1641 +/- 11 Ma - 1629 +/- 12 Ma||||Mainly I-type mafic granitoids: granodiorite and monzogranite.|
78351|Poodla Hill Suite|67653|6|Mentioned|p4|||Geological province: Curnamona Province. ||||||
78351|Poodla Hill Suite|69654|6|Mentioned|p3|||Curnamona Province.||||||
78351|Poodla Hill Suite|70657|6|Mentioned|p6 Fig.1|Statherian|Statherian||~1630Ma|||||
75849|Poolalalie Dolomite|66882|5|Briefly described|p103 Fig.3c, p113-114|Orosirian|Orosirian|New name for dolomitic units in the Lincoln-Cleve uplands, formerly mapped as Katunga Dolomite.||Darke Peak Group.||Underlies Yabmana Iron Formation, overlies Warrow Quartzite.||
28934|Poornamookinnie Member|40448|5|Briefly described|Table 3|||Informal name.||||||
39239|Port Elliot Granite|23996|6|Mentioned|p352|||Geological Province: Adelaide Fold Belt.||||||17-NOV-22
28936|Port Vincent Limestone|22541|6|Mentioned|p 29|||||||||
28936|Port Vincent Limestone|30251|4|Described|p3|||||||||
28936|Port Vincent Limestone|30828|6|Mentioned|p115|||||||||
28936|Port Vincent Limestone|32601|6|Mentioned|p672|||||||||
28936|Port Vincent Limestone|33330|2|Defined|p165|middle Miocene|late Eocene|Upper Eocene - Middle Miocene||||||
28936|Port Vincent Limestone|35689|6|Mentioned|Fig.33|||Stratigraphic correlation, St.Vincent Basin.||||||
28936|Port Vincent Limestone|41513|6|Mentioned|p45|||||||||
28936|Port Vincent Limestone|41519|6|Mentioned|p169|||||||||
28936|Port Vincent Limestone|43667|6|Mentioned|Fig.3,p12|Miocene|Oligocene|||||||
28936|Port Vincent Limestone|44133|5|Briefly described|p165 Fig. 10.11|Early Miocene|Early Oligocene|Of The Port Willunga Formation. Geological Province: Saint Vincent Basin. ||||||
28936|Port Vincent Limestone|60958|5|Briefly described|Map Legend|Miocene|Oligocene|Sandy bryozoal limestone and silty limestone. Transitional to Port Willunga Formation. Geological Province: Saint Vincent Basin.||||||
28936|Port Vincent Limestone|61121|5|Briefly described|Map legend|Miocene|Oligocene|Sandy bryozoal limestone and silty limestone, transitional into Port Willunga Formation below. Geological  Province: St. Vincent Basin.||||||06-JUN-05
28936|Port Vincent Limestone|65375|4|Described|p34 Fig.7, p36, p50.|Miocene|Miocene|Equivalent (based on similarity of fossils) to middle and upper members of Port Willunga Formation. Basal part was deposited in a half-graben shaped channel within Rogue Formation. Shown as Miocene in Fig 7.||||Transitional into Port Willunga Formation. Overlies Rogue Formation north of Port Vincent, but grades into it north of Port Julia.|Sandy bryozoan limestone.|
28936|Port Vincent Limestone|67462|5|Briefly described|Map legend.|Miocene|Miocene|Eastern Saint Vincent Basin.||||||
28936|Port Vincent Limestone|70382|5|Briefly described|p28, p29 Fig 3, p30|Miocene|Oligocene|Geological province: Troubridge Basin.||||Conformably overlies Rogue Formation.|Bryozoal limestone, arenaceous.|
28936|Port Vincent Limestone|70660|6|Mentioned|p20|||||||Equivalent to the Port Willunga Formation.||
26109|Port Willunga Formation|22525|5|Briefly described|p35|Oligocene|Eocene|||||||
26109|Port Willunga Formation|22528|6|Mentioned|p43 Fig2||Oligocene|||||||
26109|Port Willunga Formation|22541|4|Described|p 29, Fig 1, 3|Middle Miocene|Late Eocene|||||||
26109|Port Willunga Formation|22587|6|Mentioned|p79 Fig.7|Middle Miocene|Late Eocene|||||||
26109|Port Willunga Formation|22822|6|Mentioned|P11||Tertiary|||||||
26109|Port Willunga Formation|23010|6|Mentioned|p340||Oligocene|||||||
26109|Port Willunga Formation|23418|6|Mentioned|p14 Fig.4|||Informally used as "Upper Port Willunga Formation".||||||
26109|Port Willunga Formation|23489|4|Described|p44|Oligocene|Eocene|||||||
26109|Port Willunga Formation|23731|6|Mentioned|p23|||Fossiliferous limestone.||||||
26109|Port Willunga Formation|23768|5|Briefly described|p28 Fig.5|Early Miocene|Early Oligocene|Geological Province: St Vincent Basin.  See also p57, p63, p103-105.||||||30-MAR-05
26109|Port Willunga Formation|24102|5|Briefly described|p132|Early Miocene|Oligocene|||||||
26109|Port Willunga Formation|24566|5|Briefly described|p111, p114 Fig. 8|Early Miocene|Oligocene|Overlain by Pooraka Formation. Limestone units. Equivalent of Mannum Limestone.||||||
26109|Port Willunga Formation|30250|6|Mentioned|p2|||See also Fig.2||||||
26109|Port Willunga Formation|35542|6|Mentioned|p2|||||||||
26109|Port Willunga Formation|35689|2|Defined|p20|early Miocene|Oligocene|Late Eocene to Early Miocene.||||||01-JUL-08
26109|Port Willunga Formation|36127|4|Described|p11|||See also p7.||||||23-JUN-08
26109|Port Willunga Formation|36244|6|Mentioned|p2|||Redefined by Cooper 1979.||||||
26109|Port Willunga Formation|36500|6|Mentioned|Fig.4|||||||||
26109|Port Willunga Formation|37324|6|Mentioned|p11|||||||||
26109|Port Willunga Formation|37852|6|Mentioned|p2|||||||||
26109|Port Willunga Formation|37853|6|Mentioned|Fig.2|||||||||
26109|Port Willunga Formation|38107|4|Described|p34|||||||||
26109|Port Willunga Formation|38621|6|Mentioned|Table 1|||Refers Cooper 1979.||||||
26109|Port Willunga Formation|38622|6|Mentioned|p8|||||||||
26109|Port Willunga Formation|38699|6|Mentioned|p12|||See also P19||||||
26109|Port Willunga Formation|38702|6|Mentioned|p127|||||||||
26109|Port Willunga Formation|39351|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
26109|Port Willunga Formation|39352|6|Mentioned|Map legend|middle Miocene|middle Eocene|Middle Eocene to Middle Miocene||||||
26109|Port Willunga Formation|39522|6|Mentioned|p85|||||||||
26109|Port Willunga Formation|40152|6|Mentioned|p10|||||||||
26109|Port Willunga Formation|40238|6|Mentioned|p324|||||||||
26109|Port Willunga Formation|40429|6|Mentioned|Fig.4|||||||||
26109|Port Willunga Formation|40453|5|Briefly described|p57|||||||||
26109|Port Willunga Formation|40877|5|Briefly described|p50|||||||||
26109|Port Willunga Formation|40969|6|Mentioned|p10|||||||||
26109|Port Willunga Formation|40970|6|Mentioned|p16|||||||||
26109|Port Willunga Formation|41025|5|Briefly described|p165|||Mention Fig.2||||||
26109|Port Willunga Formation|41076|6|Mentioned|p63|||||||||
26109|Port Willunga Formation|41495|5|Briefly described|Table 5|||||||||
26109|Port Willunga Formation|41505|6|Mentioned|p2|||||||||
26109|Port Willunga Formation|41513|6|Mentioned|p40|||||||||
26109|Port Willunga Formation|41517|6|Mentioned|p137|||||||||
26109|Port Willunga Formation|41519|6|Mentioned|p175|||||||||
26109|Port Willunga Formation|41520|5|Briefly described|Fig.2|||||||||
26109|Port Willunga Formation|41522|6|Mentioned|p247|||||||||
26109|Port Willunga Formation|41626|6|Mentioned|p54|||||||||
26109|Port Willunga Formation|42473|6|Mentioned|p64|||||||||
26109|Port Willunga Formation|42498|5|Briefly described|Map Legend|Miocene|Oligocene|||||||
26109|Port Willunga Formation|42506|5|Briefly described|Map legend|Miocene|Oligocene|Age Tertiary (Oligocene to Miocene)||||||
26109|Port Willunga Formation|42733|5|Briefly described|map legend|Tertiary||||||||
26109|Port Willunga Formation|43026|6|Mentioned|p589|||||||||
26109|Port Willunga Formation|43053|5|Briefly described|Map Legend|Miocene|Eocene|Marine limestone. Geological Province: St Vincent Basin.||||||25-MAY-05
26109|Port Willunga Formation|43258|5|Briefly described|Map Legend|Miocene|Eocene|||||||
26109|Port Willunga Formation|43298|6|Mentioned|Map Legend|Miocene|Eocene|||||||
26109|Port Willunga Formation|43667|6|Mentioned|Fig.3,p12|Miocene|Oligocene|||||||
26109|Port Willunga Formation|43675|6|Mentioned|340|||||||||
26109|Port Willunga Formation|43844|5|Briefly described|16||Tertiary|Age 35-15 Ma. Thickness 30-40m. Polyzoal.||||||
26109|Port Willunga Formation|44133|5|Briefly described|p165 Fig. 10.11, 168|Middle Miocene|Late Eocene|Geological Province: Saint Vincent Basin. Thickness: 33m. Includes: Aldinga Member, Ruwarung Member.||||||
26109|Port Willunga Formation|44145|6|Mentioned|p556|||Similar chert nodules to Wilson Bluff Limestone may be attributed to oceanic cooling and circulation changes. ||||||
26109|Port Willunga Formation|60538|5|Briefly described|p479 Fig. 18|Oligocene|Eocene|Geological Province: Saint Vincent Basin. Includes: Ruwarung Member, Aldinga Member.||||||
26109|Port Willunga Formation|60953|5|Briefly described|Map Legend|Miocene|Eocene|Geological Province: Saint Vincent Basin.||||||
26109|Port Willunga Formation|60958|5|Briefly described|Map Legend|Miocene|Eocene|Thick bedded bryozoan rich limestone, silty and sandy locally. Skeletal limestone, calcareous sandstone, minor marls. Geological Province: Saint Vincent Basin.||||||
26109|Port Willunga Formation|61108|5|Briefly described|map legend|Miocene|Eocene|Geological Province: St Vincent Basin.||||||31-MAY-05
26109|Port Willunga Formation|61121|5|Briefly described|Map legend|Miocene|Eocene|Thick-bedded, bryozoan-rich limestone, silty and sandy locally; lower sandy, skeletal lst and calcareous sst; middle pink-brown massive to thick-bedded fossiliferous with minor marl layers; upper part bleached and silty.  Geol. Prov: St. Vincent Basin.||||||
26109|Port Willunga Formation|61155|5|Briefly described|p17|Middle Miocene|Early Oligocene|Includes the Aldinga and Ruwarung Members, Pirramimma Sand Member, Munno Para Clay Member. Bryozoal limestones and marls. Age: 37-14Ma. Max. thickness: 250m. Geological Province: St Vincent Basin. See also p3, p4.||||||
26109|Port Willunga Formation|62896|6|Mentioned|p88|||Contains cytheropterine ostracods.||||||07-FEB-11
26109|Port Willunga Formation|62899|6|Mentioned|p46|Oligocene|Oligocene|In South Australia.||||||
26109|Port Willunga Formation|63222|6|Mentioned|p40|||Correlated with Coobowie Limestone.||||||01-MAR-10
26109|Port Willunga Formation|63739|5|Briefly described|p46|Oligocene|Oligocene|Contains ostracod assemblages in South Australia.||||||01-JUL-08
26109|Port Willunga Formation|63740|6|Mentioned|p88|||Contains cytheropterine ostracods.||||||07-FEB-11
26109|Port Willunga Formation|64282|5|Briefly described|Map legend|Miocene|Miocene|Geol.prov: St Vincent Basin.Thick-bedded bryozoan-rich limestone; silty and sandy locally. Lower sandy skeletal limest. + calcareous sst; middle pinkish-brown massive to thick-bedded fossiliferous limest. + minor marl layers; upper bleached, silty limesto||||||23-JUN-08
26109|Port Willunga Formation|64397|5|Briefly described|p233, p245 Fig. 11.  |Oligocene|Oligocene|Comprises Ruwarung and Aldinga Members. See also Fig. 2. Detailed lithological chart presented - p237, Fig. 5. Geological province: St Vincent Basin.||||||
26109|Port Willunga Formation|64705|6|Mentioned|p80 Fig. 7d (photo)|Miocene|Oligocene|||||||04-DEC-08
26109|Port Willunga Formation|64993|5|Briefly described|p24, p29 Fig. 5|Early Oligocene|Early Oligocene|Contains Aldinga and  Ruwarung Members. Geological province: St Vincent Basin. Contains fossil assemblages of a new species of Lyncina (Austrocypraea) - cowries.||||||26-MAR-09
26109|Port Willunga Formation|65375|4|Described|p32, pp35-37, p54.|Miocene|Eocene|Middle and upper parts are equivalent to Melton Limestone and Point Turton Limestone. Locally capped with calcrete. About 1.5 Mt/y quarried at Klein Point for cement manufacture. Age from Fig 7.|||Includes Aldinga and Ruwarang Members.|Unconformably overlies Cape Jervis Formation and Blanche Point Limestone. Is unconformably overlain by Hallett Cove Sandstone and Hindmarsh Clay.|Thick-bedded, bryozoan-rich, locally sandy or silty limestone.|
26109|Port Willunga Formation|65891|5|Briefly described|p221-222.|Paleogene|Paleogene|St Vincent Basin. Includes Aldinga and Ruwarung Members. Overlies Chinaman Gully Formation.||||||
26109|Port Willunga Formation|66131|6|Mentioned|p242 Fig.2|Miocene|Eocene|Late Eocene to Middle Miocene in age (from Fig.2 - stratigraphic correlation chart).|||Includes Aldinga and Ruwarung Members.|||
26109|Port Willunga Formation|66194|5|Briefly described|p584|||St Vincent Basin. Marine.||||||09-MAR-12
26109|Port Willunga Formation|67462|5|Briefly described|Map legend.||Eocene|Eastern Saint Vincent Basin.|||Includes Aldinga and Ruwarung Members.|||
26109|Port Willunga Formation|68715|6|Mentioned|p31 Fig.5|Burdigalian|Aquitanian|St Vincent Basin.|||Aldinga, Ruwarung Members.|||07-APR-17
26109|Port Willunga Formation|68811|6|Mentioned|p87, p88, p128 tbl 15, p154 app 1|Tertiary|Tertiary|||||Overlies the Blanche Point Formation.||15-APR-20
26109|Port Willunga Formation|70660|5|Briefly described|p3, p9-p12, p20-p21|Miocene|Oligocene|See also  p20 fig 11a, p21 fig 11c, p22, p25, p30, p32, p38, p40, p43, p46.|||Includes the Aldinga Member and Ruwarung Member.|Overlies the Janjukian Unit. Unconformably overlies the Heatherdale Shale. Overlain by the Hallett Cove Sandstone. Equivalent to the Port Vincent Limestone.||
26109|Port Willunga Formation|70722|5|Briefly described|p217-218,228|Late Oligocene|Early Oligocene|Of St. Vincent Basin. Also referred to as Willunga Formation on p228. Biosiliceous.|||Includes Janjukian Unit, Ruwarung member and Aldinga Member.|Underlain by Chinaman Gully Formation.||
26109|Port Willunga Formation|72450|5|Briefly described|Brochure, Brochure map|Oligocene|Oligocene||||||Fossiliferous Limestone.|
26109|Port Willunga Formation|73107|5|Briefly described|Map legend.|Miocene|Miocene||||||Thick-bedded bryozoan-rich limestone, silty and sandy locally. Lower sandy, skeletal limestone and calcareous sandstone; middle pink-brown massive to thick-bedded fossiliferous limestone with minor marl layers; upper part bleached silty limestone.|
26109|Port Willunga Formation|73188|5|Briefly described|[See comments]|Miocene|Oligocene|St Vincent Basin. Marine depositional environment[?] including several sequence boundaries. p: 319-320, 335-338, 345-346, 351, 356, 358.|||Ruwarung Member, Aldinga Member|Underlain by Chinaman Gully Formation.|Shelly calcarenite with siliceous and silty bands.|
26109|Port Willunga Formation|73292|6|Mentioned|p954|||Equivalent of the Point Turton Limestone.||||Unconformably underlies the Glanville Formation||
31509|Portee Carbonate Member|23226|2|Defined|p896||Longfordian|Laterally equivalent to Cowirra Clay and Woolpunda Marl Members. Fossil assemblage distinguishes member from other strata. Of Finniss Formation.||||||
31509|Portee Carbonate Member|63460|5|Briefly described|p840 Fig. 3|Early Miocene|Early Miocene|Of the Finniss Formation. Geological province: Murray Basin. See also the misspelt version - Potree Carbonate Member (p847).||||||
31509|Portee Carbonate Member|64237|5|Briefly described|p19 Fig. 2b|Middle Miocene|Early Miocene|Of the Finniss Formation (Murray Group). Originally introduced as a new member with the stratigraphic revision of the Murray Group up to Murray Supergroup by Lukasic and James (1998), but retained when Murray Group was reinstated.||||||
70269|Portia Formation|64741|4|Described|p301 Fig. 4, p307, p308, p314|Paleoproterozoic|Paleoproterozoic|Age: ~1705-1702Ma.Overlies undifferentiated Willyama Supergp rocks.Thickness:250m.Geol.prov: Mulyungarie Domain. Assemblage of metasediments characterised by presence of carbonate, calc-silicate minerals, alkali feldspar, etc (details p307).See also p309||||||07-FEB-11
70269|Portia Formation|64944|4|Described|p27, p31, p32|Paleoproterozoic|Paleoproterozoic|Lithologically similar to Bimba Fm - the correlation is uncertain, hence this unit is separately named. Thickness: 250m. A calcareous package, pyrite-pyrrhotite-rich, locally containing lenses of massive sulphide||||||07-FEB-11
70269|Portia Formation|66302|5|Briefly described|p36 Fig.9, p38|Statherian|Statherian|Mulyungarie Domain, Curnamona Province. Also dated at 1705 +/- 4 Ma (SHRIMP, Jagodzinski et al, 2006)|1702 +/- 6 Ma (SHRIMP U-Pb, Teale, 2000)|Willyama Supergroup|||Siltstone, calcareous siltstone and minor carbonates and tuffs.|
70269|Portia Formation|70340|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic||||||Metasiltstone, laminated; characterised by suphide (mainly pyrite), calcsilicate and minor marble. Locally tuffaceous.|
70269|Portia Formation|70405|5|Briefly described|p30|Paleoproterozoic|Paleoproterozoic||1702 Ma- 1705 Ma||||Thin tuff layer in laminated low grade metasiltstone.|
70269|Portia Formation|70657|4|Described|p7, p10, p12, p14-15, p26, p32-33, p38|Statherian|Statherian|See also p40, p59, p64-65. Conor (in prep). Curnamona Province; Mulyungarie Domain. The thick (200-300 m) sulphidic carbonate-bearing, mineralised package at the Portia, Kalkaroo and Polygonum Cu-Au-Mo Prospects. Mineralisation discussed. Tuff-bearing horizon at North Portia. Continues to the E below the Mundi Mundi Plain. Has textural evidence of evaporitic deposition. Resembles Bimba Formation. A similar age is of 1705 +/- 4 Ma (Jagodzinski et al., 2006).|1702 +/- 6 Ma (Teale, 2000).|||Underlies Saltbush Group. Overlies Curnamona Group. Equivalent to Bimba Foprmation, Ettlewood Calc-Silicate Member, and ?Cues Formation in Broken Hill Domain.|~250 m thick package of siltstone, calcareous metasiltstone, and minor carbonate. Strongly pyritic-pyrrhotitic and Pb-Zn mineralised.|
70269|Portia Formation|70658|6|Mentioned|p15|Paleoproterozoic|Paleoproterozoic|Mulyungarie Domain, Curnamona Province.|1705-1702 Ma.|||||
70269|Portia Formation|73429|5|Briefly described|p106 Fig.2, p107-108, p110, p111 Fig.6|Statherian|Statherian|Curnamona Province, Mulyungarie Domain. Correlated with Bimba Formation, alternatively correlated with Cues Formation. Characterised by metasedimentary rocks with a moderate magnetic respose at North Portia, and associated with redox boundary sulfide mineralisation. Location in text includes p112 Fig.7, p113.|c. 1705 Ma|||||
27541|Potoroo Formation|22485|4|Described|p51 , Fig 2 & p53|Tertiary|Late Cretaceous|||||||
27541|Potoroo Formation|22663|5|Briefly described|S97-1 and 2 p3|||||||||
27541|Potoroo Formation|23792|5|Briefly described|p47, Fig.D4|Maastrichtian|Campanian|Equivalent to Hammerhead Supersequence. Overlies Wigunda Formation. Unconformably overlain by Pidinga Formation. Geological Province: Bight Basin.||||||04-MAY-05
27541|Potoroo Formation|24201|5|Briefly described|p373 Fig. 2|Maastrichtian|Campanian|||||||
27541|Potoroo Formation|24338|5|Briefly described|p38 Fig. 2|Maastrichtian|Campanian|Unconformably overlain by the Pidinga Formation. Overlies the Wigunda Formation. Formation is Fm. in text. Geological Province: Bight Basin.||||||
27541|Potoroo Formation|24350|5|Briefly described|Fig. 4 Appdx|Maastrichtian|Campanian|Equivalent in part to Hammerhead Supersequence.||||||21-JAN-16
27541|Potoroo Formation|24553|5|Briefly described|p37, Figs. 7 and 10|Cretaceous|Cretaceous|Geological Province: Duntroon Sub-basin. Fluvial to paralic sandstones. Part of Hammerhead Supersequence.||||||07-FEB-11
27541|Potoroo Formation|34759|6|Mentioned|Fig.7|||Stratigraphy||||||
27541|Potoroo Formation|36244|6|Mentioned|p2|||Refers Fraser & Tilbury 1979.||||||
27541|Potoroo Formation|38221|6|Mentioned|Fig.4|||Great Australian Bight Basin||||||
27541|Potoroo Formation|42075|5|Briefly described|Fig.10 P250|||||||||
27541|Potoroo Formation|42545|4|Described|p12, p18|Maastrichtian|Coniacian|||||||
27541|Potoroo Formation|43026|5|Briefly described|Table 1,p586|||||||||
27541|Potoroo Formation|43052|5|Briefly described|Table 2.1|||||||||
27541|Potoroo Formation|43814|6|Mentioned|Fig.3,p115|||||||||
27541|Potoroo Formation|44133|5|Briefly described|p137, 141|Maastrichtian|Coniacian|Conformably overlies Wigunda Formation. Unconformably overlain by Pidinga Formation. Thickness: 580m. ||||||
27541|Potoroo Formation|49060|5|Briefly described|Fig.15|||||||||
27541|Potoroo Formation|61155|5|Briefly described|p17|||Age is pre-Cainozoic. Max. thickness: 600m. Geological Province: Great Australian Bight.||||||
27541|Potoroo Formation|61544|6|Mentioned|p367 Fig.3. |Maastrichtian|Campanian|||||Overlies Wigunda Formation.||
27541|Potoroo Formation|61630|6|Mentioned|p555 Fig. 3, p559|Paleocene|Late Cretaceous|Geological Province: Bright and Duntroon Basins.||||||07-APR-09
27541|Potoroo Formation|69297|5|Briefly described|p14 fig 2.4, p25 fig 2.9|Danian|Santonian|Ceduna and Duntroon Sub-basins. Deposited in a marine or delta environment. Good reservoir properties. See also p39 fig 2.14, p58, p60, p64. ||||Overlies the Wigunda Formation. Unconformably overlain by the Pidinga Formation.|Mudstone, sandstone and siltstone.|
27541|Potoroo Formation|70067|5|Briefly described|Ceduna: Fig.2; p1. Regional: Fig.2|Maastrichtian|Santonian|Bight Basin. Contains good quality sandstone reservoirs.||||Overlies Wigunda Formation. Is overlain by Pidinga Formation.||
33395|Price Metasediments|24508|6|Mentioned|p30|||Geological Province: Gawler Craton.||||||
33395|Price Metasediments|60707|5|Briefly described|p617-618|||Composed of thin banded phyllosilicate-quartz-garnet-opaques rock to opaques-quartz-phyllosilicate rock to calc-silicate rock to apatite-quartz-phyllosilicate rock (Schwarz 2003).  Age: 1767+/-17Ma (SHRIMP, Oliver and Fanning 1997).||||||05-MAR-15
33395|Price Metasediments|60953|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Megnetite-rich pelitic schist. Age: 1760Ma.||||||07-NOV-08
33395|Price Metasediments|61070|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Magnetite-bearing, finely layered pelitic metasediment. Type locality; Price Island. Depositional age: 1767 +/- 17Ma on tuffaceous component of sediments (U-Pb Zircon). Geological Province: Gawler Craton.||||||12-JAN-10
33395|Price Metasediments|61108|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|Magnetite-rich pelitic schist. Age: 1760 Ma.||||||07-NOV-08
33395|Price Metasediments|64130|5|Briefly described|p1378 Fig.1, p1380 Fig.2, p1381 |Paleoproterozoic|Paleoproterozoic|Eastern Gawler Craton.|1767 +/- 17 Ma (Oliver and Fanning, 1997).|||||
33395|Price Metasediments|64828|5|Briefly described|p1065 Fig. 2, p1067|Paleoproterozoic|Paleoproterozoic|Overlies Hall Bay Volcanics. Age: 1760Ma. Greenschist facies/phyllitic schists. See also p1078.||||||04-MAR-09
33395|Price Metasediments|65375|6|Mentioned|p19.|||Northern Eyre Peninsula.||||||
33395|Price Metasediments|65376|6|Mentioned|p17. |Paleoproterozoic|Paleoproterozoic|||||||
33395|Price Metasediments|65390|5|Briefly described|p20, p23 Fig.3|Statherian|Statherian|Coulta Domain, Gawler Craton. Interpreted to have been deposited during a period of crustal extension at approximately 1770 Ma.||||||27-FEB-15
33395|Price Metasediments|65485|6|Mentioned|Fig 1, p42|Palaeoproterozoic|Statherian|Western Eyre Peninsula. Maximum depositional age: ~1760 Ma. May be correlative of Wallaoo Group volcaniclastics and sediments.|||||Low grade phyllitic schist.|19-MAR-12
33395|Price Metasediments|65772|6|Mentioned|p229 Fig.2|Paleoproterozoic|Paleoproterozoic|||||||
33395|Price Metasediments|66302|6|Mentioned|p25, p33, p63|Statherian|Statherian|SHRIMP ages from Oliver and Fanning (1997). |1766 +/- 14 to 1767 +/- 16 Ma|||||
33395|Price Metasediments|66882|6|Mentioned|p102 Fig.2, p118|Statherian|Statherian|Far SW of South Australian Craton. Linked with a 1756 Ma metasedimentary succession at Cape Hunter, Antarctica.|c.1765 Ma.|||||
33395|Price Metasediments|67058|5|Briefly described|p476.|Paleoproterozoic|Paleoproterozoic||1767 +/- 17 Ma (Oliver and Fanning 1997).|||||
33395|Price Metasediments|67323|5|Briefly described|Eastern Australia Time-Space Plot|||See also p31-32. Southern Gawler Craton. Also given is an MDA of 1767 +/- 17 Ma.|~1770-1740 Ma: protolith deposition.|||||
33395|Price Metasediments|67536|5|Briefly described|Map Legend|Statherian|Statherian|Gawler Craton.|1767 +/- 17 Ma||||Iron-rich metapelite, partly tuffaceous.|
33395|Price Metasediments|69048|5|Briefly described|p1, p3-4, p60-65, p74|Paleoproterozoic|Paleoproterozoic|Described by Oliver and Fanning (1997). Occupies a narrow, c.3km-wide magnetic high zone along the western edge of Southern Eyre Peninsula. SHRIMP U-Pb maximum deposition age. An earlier deposition age of 1766 +/- 14 Ma was determined by Oliver and Fanning (1997).|1749 +/- 5 Ma.||||Phyllitic sedimentary rocks including iron-rich sediments.|
33395|Price Metasediments|69591|6|Mentioned|p105 Fig.2.99|||Appears in a diagram of the geodynamic setting of ~1870-1820 Ma eastern Australia.||||||
33395|Price Metasediments|70027|4|Described|p56-57,61,70,72-73|Statherian|Statherian|Geological province: Gawler Craton. Deposited at ca. 1765 Ma, and can be correlated to phyllites in the Cape Hunter region of Antarctica (Oliver and Fanning 1997). Zircon U-Pb SHRIMP geochronology results on p70, Sm-Nd whole rock data detailed on p70-71. Sm-Nd whole rock ages are consistent at 1749+\-5 Ma. Correlable to Cape Hunter phyllite, Commonwealth By, Antarctica. Coeval with Moonabie Formation, Wallaroo Group and significantly, Warramboo magnetite gneiss (similar U-Pb zircon and Sm-Nd isotopic data). Likely a similar sedimentary source to the Wallaroo magnetite gneiss, based on presence of spessartine garnet; and probably formed in the same basin system.|ca 1749+\-5 Ma||||Magnetite-bearing phyllitic schist; magnetite-quartz-biotite-muscovite-chlorite+\-spessartine garnet|
33395|Price Metasediments|71129|6|Mentioned|p18|Statherian|Statherian|Geological Province: Cleve-Coulta Domain, Gawler Craton. |<1760 Ma|||||
33395|Price Metasediments|71317|5|Briefly described|p16||Palaeoproterozoic|Cleve-Coulta Domains, Gawler Craton.|<1760 Ma|||||
33395|Price Metasediments|71341|6|Mentioned|p196|||Broadly geochemically similar to the Myola Volcanics, McGregor Volcanics, Cleve Group, Moonabie Formation and the Wallaroo Group. ||||||
33395|Price Metasediments|71859|5|Briefly described|p3-p4|Paleoproterozoic|Paleoproterozoic|Cleve and Coulta domains, southern Gawler Craton.|< 1760 Ma|||||
33395|Price Metasediments|71862|6|Mentioned|p3|||||||||
33395|Price Metasediments|72090|6|Mentioned|p10|Statherian|Statherian|Cleve-Coulta Domain, Gawler Craton.|<1750 Ma|||||
33395|Price Metasediments|72462|6|Mentioned|p3|Paleoproterozoic|Paleoproterozoic|Gawler Craton.||||||
33395|Price Metasediments|73026|5|Briefly described|p6, p7, p9, p18|Paleoproterozoic|Paleoproterozoic|South-western Eyre Peninsula.|c. 1770 Ma||||Schist, fine grained, pelitic, magnetite-rich.|
33395|Price Metasediments|73027|5|Briefly described|p6-p7,p9,, p18|Statherian|Statherian|Central/western Eyre Peninsula.|c. 1770 Ma||||Schist, fine-grained, pelitic, magnetite rich.|
33395|Price Metasediments|73235|6|Mentioned|p53|Statherian[?]|Statherian|Gawler Craton. Cleve and Coulta regions.|<1760 Ma|||||
83511|Prominent Hill Group|73155|5|Briefly described|p265, p277-278, p282 Fig.13, p283-284|Calymmian|Calymmian|Mount Woods Domain, southern. Not a formalised stratigraphic name, also termed Prominent Hill Mine Sequence of Freeman and Tomkinson (2010), hosts Prominent Hill orebody. Intercalated with possible Gawler Range Volcanics. Low to moderate magnetic response with smooth texture, occurs in two narrow strips. Interpreted as part of hangingwall/upper plate of Mount Woods Metamorphic Core Complex. Prominent Hill Mine Sequence used on p265, p282 Fig.13, p284.|ca. 1590 Ma maximum depositional age||||Hematite-cemented quartz conglomerate, sandstone, argillite and dolostone. Red sandstone, siltstone, dolomite, breccia, dacite and andesite; low to negligible metamorphic grade.|
24622|Prospect Hill Granite|22631|6|Mentioned|p176|Calymmian|Calymmian|||||||
24622|Prospect Hill Granite|24197|5|Briefly described|p75 Tb. 8.1|Mesoproterozoic|Mesoproterozoic|Age: 1560Ma.||||||07-FEB-11
24622|Prospect Hill Granite|42602|6|Mentioned|p19|||Name reserved.||||||
24622|Prospect Hill Granite|42624|2|Defined|p20|Mesoproterozoic||||||||
24622|Prospect Hill Granite|42885|6|Mentioned|p29|||||||||
24622|Prospect Hill Granite|43052|5|Briefly described|p153|||||||||
24622|Prospect Hill Granite|50605|5|Briefly described|p(iii), 1.4, 10.2, Table 1.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Gawler Craton & Curnamona Province. Of the Moolawatana Suite.||||||
24622|Prospect Hill Granite|68068|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Curnamona Province.||Unit in Moolawatana Suite.||Intrudes Petermorra Volcanics.|Sparsely porphyritic adamellite, dark grey, with tourmaline clots and orbicules, wispy volcanic and granitic xenoliths. Composed of microcline phenocrysts in a groundmass of orthoclase, plagioclase, bluish quartz and biotite.|
24622|Prospect Hill Granite|69019|5|Briefly described|p23, p66.|Calymmian|Calymmian|Mt. Babbage Inlier.|c.1555 Ma.||||Sparsely separated ovoid feldspar megacrysts (or ?xenocrysts) in a medium- to fine-grained matrix.|
24622|Prospect Hill Granite|69023|4|Described|p26, p35-38, p46-50, p143-144, p189|||Of Sheard et al. (1992) after informal use by Teale et al. (1989). Previously included within Mount Neill Granite Porphyry by Coats et al. (1969). Mount Babbage Inlier. Geochemistry detailed. Age unknown but younger than Petermorra Volcanics.||Unit in Moolawatana Suite.||Intrudes Petermorra Volcanics.|A distinctive, mid-grey, microperthitic microcline-porphyritic monzogranite; develops a brownish weathering rind; quartz-tourmaline clots or orbicules (30-100mm) are characteristic; weakly foliated.|
24622|Prospect Hill Granite|69562|5|Briefly described|p670 Tb.5|||Age assumed to be similar to Yerila Granite.|1556 +/- 4 Ma (Sheard et al. 1992).||||Biotite granite.|
24622|Prospect Hill Granite|70384|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Composed of scattered anhedral to round microcline phenocrysts set in a groundmass of subequal amounts of orthoclase, plagioclase,  bluish quartz and ~10% biotite. Accessory tourmaline, fluorite, monazite and allanite.||||Intrudes Petermorra Volcanics.|Sparsely porphyritic adamellite, dark grey, with tourmaline clots and orbicules, wispy volcanic and granitic xenoliths. Leucocratic near upper intrusive contact with Petermorra Volcanics at Prospect Hill.|17-JAN-19
24622|Prospect Hill Granite|72459|6|Mentioned|p63, p66, p73, p100|Mesoproterozoic|Mesoproterozoic|||Moolawatana Suite||||
27223|Pualco Tillite|22510|5|Briefly described|table 1, p36,38|||Of the Yudnamutana Subgroup.  Olary Region. Age: Sturtian||||||13-OCT-04
27223|Pualco Tillite|22631|6|Mentioned|p177|Cryogenian|Cryogenian|||||||
27223|Pualco Tillite|23250|5|Briefly described|p1124 Fig.2||Cryogenian|of Umberatana Group.||||||
27223|Pualco Tillite|23351|5|Briefly described|283|Neoproterozoic|Neoproterozoic|||||||
27223|Pualco Tillite|23477|5|Briefly described|p49 Fig 3|Neoproterozoic|Neoproterozoic|Of Yudnamutana Subgroup. Geological Province: Curnamona Province.||||||
27223|Pualco Tillite|24546|5|Briefly described|p2 - 3 Fig.2|Neoproterozoic|Neoproterozoic|Of Umberatana Group. Geological Province: Adelaide Fold Belt.||||||16-JAN-08
27223|Pualco Tillite|30178|6|Mentioned|p20|||See also P20.||||||
27223|Pualco Tillite|30810|2|Defined|p2|Adelaidean|Adelaidean|||||||
27223|Pualco Tillite|35200|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
27223|Pualco Tillite|35232|6|Mentioned|p5|||See also Table 1.||||||
27223|Pualco Tillite|36838|6|Mentioned|Fig.1|||||||||
27223|Pualco Tillite|37238|6|Mentioned|p367|||||||||
27223|Pualco Tillite|37461|4|Described|p339|||See also Table 5.I||||||
27223|Pualco Tillite|37932|4|Described|p540|||||||||
27223|Pualco Tillite|38157|6|Mentioned|Table IV|||||||||
27223|Pualco Tillite|39344|6|Mentioned|Map legend|Precambrian|Precambrian|Sturtian||||||
27223|Pualco Tillite|39352|6|Mentioned|Map legend|Precambrian|Precambrian|Sturtian||||||
27223|Pualco Tillite|40294|6|Mentioned|p41|||||||||
27223|Pualco Tillite|40914|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
27223|Pualco Tillite|41404|6|Mentioned|p121|||||||||
27223|Pualco Tillite|41405|3|Fully described|p134|||||||||
27223|Pualco Tillite|42090|5|Briefly described|p25|||||||||
27223|Pualco Tillite|42098|5|Briefly described|p53|||||||||
27223|Pualco Tillite|42222|5|Briefly described|p15|||||||||
27223|Pualco Tillite|42272|6|Mentioned|Fig.2 P400|||||||||
27223|Pualco Tillite|42720|5|Briefly described|map legend|Sturtian||||||||
27223|Pualco Tillite|42813|4|Described|p17|||Of Umberatana Group.||||||30-SEP-08
27223|Pualco Tillite|43052|5|Briefly described|p183,Table 6.1|||||||||
27223|Pualco Tillite|43086|6|Mentioned|Appendix, Stop 7|||||||||12-JUL-16
27223|Pualco Tillite|43845|5|Briefly described|Fig3 p43, 42||Neoproterozoic|In Umberatana Group||||||12-JUL-16
27223|Pualco Tillite|45155|6|Mentioned|p26|||||||||
27223|Pualco Tillite|46865|6|Mentioned|p50|||||||||
27223|Pualco Tillite|60959|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Of the Yudnamutana Subgroup. Blue-grey gritty siltstone and minor thin sandstone with pebble to boulder sized glacial clasts; matrix supported diamictite.||||||
27223|Pualco Tillite|61732|5|Briefly described|p28 Fig. 13|Sturtian|Sturtian|Of the Yudnamutana Subgroup (Umberatana Group). Geological Province: Adelaide Rift Complex.||||||07-FEB-11
27223|Pualco Tillite|62592|5|Briefly described|p50 Table 5.1, p58.|Sturtian|Sturtian|Adelaide Geosyncline. Combined thickness (with Benda Siltstone) of about 3 km.||Basal unit in Yudnamutana Subgroup.||Unconformably overlies Burra Group. Is overlain by Benda Siltstone.|Diamictite, quartzite, ironstone.|
27223|Pualco Tillite|62724|5|Briefly described|p17 Fig. 4|Sturtian|Sturtian|Of Yudnamutana Subgp (Umberatana Gp). Contains basal diamictite, quartzite, ironstone - detailed lithology given (p19). Disconformably overlies Belair Subgp; interfingering contact with Benda Siltst above. Max. thick: 200m. See also p16 Fig. 2.||||||07-FEB-11
27223|Pualco Tillite|62903|6|Mentioned|p729|Sturtian|Sturtian|Adelaide Rift Complex. Sturtian glaciation (Preiss et al. 1998) correlates with Areyonga Formation. Presented in text as Sturt-Appila-Pualco-Bolla Bollana-Merirjina Tillites.||Yudnamutana Subgroup||Sturtian glacial units overlain by Tapley Hill Formation||
27223|Pualco Tillite|63102|5|Briefly described|p8|Neoproterozoic|Neoproterozoic|Geological province: Curnamona Province.||Unit of the Yudnamutana Subgroup.|||Diamictite, quartzite, ironstone.|22-OCT-19
27223|Pualco Tillite|65925|5|Briefly described|Appendix 2.||||||||Siltstone, dark grey, calcareous, with scattered quartz grains; quartzite, tillite and minor siltstone; green-grey tillite.|
27223|Pualco Tillite|67030|6|Mentioned|p409 Fig. 2|Cryogenian|Cryogenian|Oldest unit shown in SE Flinders Ranges.||||Overlain by Banda Siltstone.||26-APR-12
27223|Pualco Tillite|68276|6|Mentioned|p69|||Flinders Ranges.|||||Diamictite complex.|
27223|Pualco Tillite|70031|5|Briefly described|p245|Cryogenian|Cryogenian|Adelaide Geosyncline. Associated with Sturtian glaciation.||Unit of Yudnamutana Subgroup.||Overlain by Benda Siltstone. Laterally equivalent to Holowilena Ironstone.||
27223|Pualco Tillite|70082|6|Mentioned|p2|Cryogenian|Cryogenian|Flinders Ranges. Contains marine till.||||||
27223|Pualco Tillite|70323|4|Described|p212-214,220,222|Cryogenian|Cryogenian|Central Flinders Ranges, Adelaide Geosyncline. Associated with Sturtian glaciation. Typically contains evidence of soft-sediment deformation. Likely a glaciomarine deposition under an extensive floating ice-sheet during the extreme glaciation of the initial Sturtian glacial event (Preiss, 1987).|c. 660 Ma|Unit of Yudnamutana Subgroup.||Passes gradationally into Holowilena Ironstone. Basal unit of the Yudnamutana Subgroup.|Massive diamictites with boulders (lithologies include quartzite, dolomite, and granite) , siltstones, sandstones, and carbonates.|
27223|Pualco Tillite|70405|5|Briefly described|p14 figure 6, p52, p79, p97|Neoproterozoic|Neoproterozoic|||Yudnamutana Subgroup||Underlies Benda Siltstone.|Massive, clast poor, pebble sized, matrix supported diamictite intercalated with clean, medium to coarse grained, tabular and trough cross bedded sandstone and quartzite; ironstone also present.|
27223|Pualco Tillite|70407|5|Briefly described|p103 Fig 2|Neoproterozoic|Neoproterozoic|Age: Sturtian.||Of Umberatana Group.||||
27223|Pualco Tillite|70657|5|Briefly described|p9 Fig.3|Neoproterozoic|Neoproterozoic|||Yudnamutana Subgroup|||Diamictite, quartzite, ironstone.|
27223|Pualco Tillite|70658|6|Mentioned|p14|Neoproterozoic|Neoproterozoic|||Yudnamutana Subgroup.|||Diamictite, quartzite, ironstone.|
27223|Pualco Tillite|72449|5|Briefly described|p1, p2 Map Legend|Neoproterozoic|Neoproterozoic|Glacially derived sediment. Shown as part of diapir formation diagram, p1.|700 Ma.|||Overlies Burra Group ?unconformably, and underlies Holowilena Ironstone.|Grey-blue gritty siltstone and minor thin sandstone with pebble to boulder-size glacial clasts.|
27223|Pualco Tillite|73093|5|Briefly described|map legend|Neoproterozoic|Neoproterozoic||||||Blue-grey gritty siltstone and minor thin sandstone with pebble to boulder sized glacial clasts; tillite; ironstone.|09-DEC-21
40391|Puttapa Conglomerate|24484|5|Briefly described|p803 Fig. 3|Neoproterozoic|Neoproterozoic|Overlies the Wonoka Formation. Overlain by the Bonney Sandstone.||||||
26114|Pyap Member|22495|6|Mentioned|P220|||||||||
26114|Pyap Member|22773|5|Briefly described|Fig24.5p350|Early Cretaceous|Early Cretaceous|||||||
26114|Pyap Member|22799|3|Fully described|p20|Aptian|Aptian|Monash Formation||||||
26114|Pyap Member|22857|5|Briefly described|p548 App.1 Tb.A1.12|Albian|Aptian|Of the Monash Formation. Weakly cemented sandstone, mudstone, coal and conglomerate. Max. thickness: 65m. Geological Province: Berri Basin. See also p350 Fig.24.5.||||||
26114|Pyap Member|22887|4|Described|Table 5 p31|Early Cretaceous|Early Cretaceous|See also Fig.5 p12.  Renmark Trough.||||||
26114|Pyap Member|22893|5|Briefly described|table5 fig4||Early Cretaceous|||||||
26114|Pyap Member|23836|5|Briefly described|p93|Cretaceous|Cretaceous|Of Monash Formation. Geological Province: Murray Basin.||||||
26114|Pyap Member|24551|6|Mentioned|p270|||Of the Monash Formation.||||||
26114|Pyap Member|33488|2|Defined|p8|Early Cretaceous|Early Cretaceous|See also p9.||||||01-NOV-22
26114|Pyap Member|33490|4|Described|p10|||Aptian. See also p23.||||||01-NOV-22
26114|Pyap Member|35232|6|Mentioned|Table.2|||||||||
26114|Pyap Member|39211|6|Mentioned|p38|||Fig.23||||||
26114|Pyap Member|42966|1|Redefined|Table 7 p67|Aptian|Aptian|of Monash Formation.||||||
26114|Pyap Member|43052|5|Briefly described|Table 2.1|||of Monash Formation||||||
26114|Pyap Member|43218|4|Described|Fig.3 p22, p27|Aptian|Aptian|Of Monash Formation,||||||
26114|Pyap Member|44133|5|Briefly described|p127|Cretaceous|Cretaceous|Of the Monash Formation. ||||||
26114|Pyap Member|44191|5|Briefly described|Map Legend||Early Cretaceous|||||||
26114|Pyap Member|49040|6|Mentioned|p8|||||||||
26114|Pyap Member|61314|5|Briefly described|p123, p129|Aptian|Aptian|Basal unit of Monash Formation. Fluvial to marine deposits - of sandstone interbedded with minor mudstone and siltstone, coal and conglomerate; possesses good reservoir characteristics. Overlain by the Merreti Member. Geol.Prov: western Murray Basin.||||||
26114|Pyap Member|73228|5|Briefly described|p50-54|Aptian|Aptian|Berri Basin. Changes upwards from non-marine fluvial to nearshore marine deposits. Identified in Cooltong 1, Berri North 1, Nadda 1, and Overland Corner 1 drillholes. Distribution appears to broadly follow embayment structures.||Monash Formation.||Underlain[?] by Urana Formation. Overlain by Merreti Member.|Transgressive succession from fluviolacustrine medium to very coarse grained pebbly quartz sandstone and minor coal to nearshore marine deposits of claystone, siltstone and clayey fine sandstone.|01-NOV-22
26114|Pyap Member|73229|5|Briefly described|p66-68, p70, p74|Early Cretaceous|Early Cretaceous|Berri Basin. [Analysed using pXRF; see article].||Monash Formation.|||Transgressive succession from fluviolacustrine medium to very coarse grained pebbly quartz sandstone and minor coal to nearshore marine deposits of claystone, siltstone and clayey fine sandstone.|01-NOV-22
75704|Radium Creek Group|66518|6|Mentioned|p19 Fig.4.|Mesoproterozoic|Mesoproterozoic|Curnamona Province. This name is a revision of Radium Creek Metamorphics and is in the process of being formalised.||||||06-FEB-14
75704|Radium Creek Group|67540|6|Mentioned|p25|||Formerly Radium Creek Metamorphics. Mount Painter Inlier of NW Curnamona Province.|c.1600-1590 Ma (Fraser and Neumann 2010).|||||
75704|Radium Creek Group|68713|5|Briefly described|p19, p22|Calymmian|Calymmian||ca. 1590 Ma|||Intruded by the Moolawatana Suite.|Crystalline metasediments.|
75704|Radium Creek Group|69019|5|Briefly described|p14-19, p64-65, p70, p133, p141.|Calymmian|Calymmian|Curnamona Province. Redefined; includes former Radium Creek Metamorphics excluding meta-igneous rocks. Comprises 5 (un-named) lithotypes. Age from detrital zircons. At least 4 deformational fabrics.|c.1590 Ma max. (Neumann et al. 2009).|||Intruded by Terrapinna and Wattleowie Granites and Mudnawatana Tonalite.|Quartz-feldspar-mica schist; psammitic and pelitic schist; quartzite; calc-silicate metasomatite; migmatitic gneiss.|
75704|Radium Creek Group|69650|6|Mentioned|p58|||||||||
75704|Radium Creek Group|70383|5|Briefly described|p44|Mesoproterozoic|Mesoproterozoic|Basement to the Mount Painter Inlier.|||Freeling Heights Quartzite.|Intruded by Coulthard and Moolawatana Suites.|Strongly foliated quartz-feldspar-biotite gneisses and schists, in part migmatitic, representing metapelites, metapsammites and felsic meta-igneous rocks, as well as thick, partly pebbly and cobbly quartzite units.|
75704|Radium Creek Group|70384|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Also includes eight un-named, separately mapped facies consisting mainly of gneiss, schist, quartzite and granite. Maximum depositional ages 1595-1580 Ma.|||Include Brindana Schist; Yagdlin Phyllite; Freeling Heights, Mount Adams Quartzites.||Metasediments: quartzite, schist, gneiss, calc-silicate rock.|04-FEB-16
75704|Radium Creek Group|70659|5|Briefly described|p5|Mesoproterozoic|Mesoproterozoic|Moolawatana Domain, Curnamona Province.|1600-1580 Ma|||||
75704|Radium Creek Group|70858|6|Mentioned|p31|||Mount Painter area, Curnamona Province.||||||
75704|Radium Creek Group|72949|6|Mentioned|p36|Statherian|Statherian|Curnamona Province. Mount Painter.||||||
75704|Radium Creek Group|73251|6|Mentioned|p35-36|Mesoproterozoic|Calymmian|Curnamona Province, Mount Painter and Mount Babbage inliers. Includes uraniferous crystalline rock.|Less than 1595 Ma|||||
75704|Radium Creek Group|74367|6|Mentioned|p23|||Curnamona Province.||||||
75704|Radium Creek Group|75063|6|Mentioned|p93, p94 Fig.2|Mesoproterozoic|Mesoproterozoic|Curnamona Province. Underwent repeated strong deformation. Intruded by minor pegmatite dykes and plutons.|1595-1580 Ma (Armit et al., 2014).||||Metasedimentary rocks.|
27885|Ramsay Limestone|22643|5|Briefly described|p191, fig3,6|Early Cambrian|Early Cambrian|||||||
27885|Ramsay Limestone|22766|5|Briefly described|Fig.2 p561|Early Cambrian|Early Cambrian|||||||
27885|Ramsay Limestone|23155|6|Mentioned|p9|||Equivalent to the Kalladeina Formation (eastern Warburton Basin).||||||
27885|Ramsay Limestone|23818|5|Briefly described|p87 Fig.33|Cambrian|Cambrian|||||||
27885|Ramsay Limestone|23981|5|Briefly described|p23,  p40|Toyonian|Toyonian|Unconformably overlies Minlaton Formation; conformably overlies Parara Limestone. Transgressive marine deposits. Blue-grey argillaceous limestone; richly fossiliferous. Geological Province: Stansbury Basin. See also p8-9 Fig. 4, p39 Fig. 12.||||||
27885|Ramsay Limestone|24465|5|Briefly described|p345 Fig.2|Cambrian|Cambrian|Geological Province: Stansbury Basin.||||||19-JAN-05
27885|Ramsay Limestone|29832|6|Mentioned|p151|||||||||
27885|Ramsay Limestone|29833|6|Mentioned|p142|||||||||
27885|Ramsay Limestone|29841|4|Described|Fig.2|||||||||
27885|Ramsay Limestone|29842|4|Described|p123|||||||||
27885|Ramsay Limestone|30374|6|Mentioned|Fig.3|||Middle Cambrian age. Correlation||||||
27885|Ramsay Limestone|30801|6|Mentioned|p5|||Table P5-6||||||
27885|Ramsay Limestone|33332|6|Mentioned|p11|||See also P14. M.Camb.||||||
27885|Ramsay Limestone|33471|6|Mentioned|Fig.1|||||||||
27885|Ramsay Limestone|33972|6|Mentioned|p13|||||||||
27885|Ramsay Limestone|34612|6|Mentioned|Fig.33|||Correlation chart. Cambrian||||||
27885|Ramsay Limestone|35255|6|Mentioned|Fig.8|||||||||
27885|Ramsay Limestone|38068|6|Mentioned|p69|||||||||
27885|Ramsay Limestone|39352|6|Mentioned|Map legend|Late Cambrian|Middle Cambrian|Middle to Late Cambrian||||||
27885|Ramsay Limestone|40003|5|Briefly described|Table 12|||||||||
27885|Ramsay Limestone|40217|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
27885|Ramsay Limestone|40856|6|Mentioned|Fig.23.6|||||||||
27885|Ramsay Limestone|41526|6|Mentioned|p61|||||||||
27885|Ramsay Limestone|42222|6|Mentioned|Table 1 P4|||||||||
27885|Ramsay Limestone|42225|4|Described|p223|||||||||
27885|Ramsay Limestone|42269|6|Mentioned|Fig.1 P335|||||||||
27885|Ramsay Limestone|42731|5|Briefly described|map legend|Middle Cambrian||||||||
27885|Ramsay Limestone|43053|5|Briefly described|Map Legend|Cambrian|Cambrian|Shallow marine to terrestrial redbeds, peritidal to marine limestone.||||||25-MAY-05
27885|Ramsay Limestone|43258|5|Briefly described|Map Legend||Cambrian|||||||
27885|Ramsay Limestone|43298|6|Mentioned|Map Legend||Cambrian|||||||
27885|Ramsay Limestone|44133|5|Briefly described|p4 Fig. 7.2, 17, 28|Early Cambrian|Early Cambrian|Geological Province: Stansbury Basin.||||||
27885|Ramsay Limestone|44691|4|Described|map legend||Middle Cambrian|Defn on Tech.File (I/53-12). Middle Cambrian.||||||
27885|Ramsay Limestone|60953|5|Briefly described|Map Legend|Cambrian|Cambrian|Geological Province: Spencer Shelf.||||||
27885|Ramsay Limestone|60958|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Flaggy to nodular, thin to medium-bedded silty limestone with basal sandy oolitic grainstone and bioclastic packstone.||||||14-APR-05
27885|Ramsay Limestone|60990|6|Mentioned|p85|||Faunal links with Antarctica.||||||
27885|Ramsay Limestone|61108|5|Briefly described|map legend|Cambrian|Cambrian|Shallow marine to terrestrial redbeds; peritidal to marine limestone. Geological Province: Spencer Shelf.||||||03-JUN-05
27885|Ramsay Limestone|61121|5|Briefly described|Map legend|Early Cambrian|Early Cambrian|Flaggy to nodular, thin to medium bedded silty limestone with basal sandy oolitic grainstone and bioclastic packstone.  Age is Toyonian. Geological Province: Stansbury Basin.||||||06-JUN-05
27885|Ramsay Limestone|62787|5|Briefly described|p82, p82 Fig. 3|Early Cambrian|Early Cambrian|Geological Province: Stansbury Basin (SA).||||||07-FEB-11
27885|Ramsay Limestone|63569|6|Mentioned|p123|Cambrian|Cambrian|Contains lingulate brachiopods that correlate with Redlichia guizhouensis Zone of China.||||||
27885|Ramsay Limestone|65375|4|Described|p27 Fig.5, p30, pp54-55.|Cambrian|Cambrian|Up to 109m thick. Contains Redlichia trilobites, Helcionella and Chancelloria, suggesting Toyonian age. Contains only minor galena, sphalerite and chalcopyrite mineralisation. Possible hydrocarbon source rock (TOC = 1.34%).||||Unconformably overlies Minlaton Formation. Is overlain by Corrodgery Formation.|Flaggy to nodular, thin- to medium-bedded silty limestone with basal sandy ooid grainstone and bioclastic packstone.|
27885|Ramsay Limestone|65686|6|Mentioned|p413, 415|Early Cambrian|Early Cambrian|Stansbury Basin, Yorke Peninsula.||||||
27885|Ramsay Limestone|65892|5|Briefly described|p9 Fig.4. |Early Cambrian|Early Cambrian|Yorke Peninsula.||||Overlies Minlaton Formation. Is overlain by Corrodgery Formation.||
27885|Ramsay Limestone|67536|6|Mentioned|Map Legend||||||||Peritidal to marine limestone.|01-APR-14
27885|Ramsay Limestone|68735|6|Mentioned|p233 Fig.2, p235 Fig.3|Early Cambrian|Early Cambrian|Stansbury Basin.||||||
27885|Ramsay Limestone|68993|6|Mentioned|p544 Fig.1|Early Cambrian|Early Cambrian|Yorke Peninsula.||||||
27885|Ramsay Limestone|70752|6|Mentioned|p133|||Brachiopod fossil briefly discussed.||||||
27885|Ramsay Limestone|70833|5|Briefly described|p200|Cambrian|Cambrian|Of Western Stansbury Basin.||||Underlain by Minlaton Formation.||
27885|Ramsay Limestone|71102|5|Briefly described|p254|||Of Stansbury Basin. Intersected in Stansbury Town 1 (drill core 10, 981.5-984.5 m), and named by Daily (1968). Contains single sclerite of S. crenulatus (Brock and Cooper 1993). Correlable to Wirrealpa Limestone (Arrowie Basin).|||||Dark-grey mottled limestone.|
27885|Ramsay Limestone|73092|6|Mentioned|p2|Cambrian|Neoproterozoic|||||||
72575|Raven Hill Subgroup|62993|6|Mentioned|p2-p4,12-15, p21, 37, 39, 43|Paleoproterozoic|Paleoproterozoic|Shown as both Raven Hill Subgroup and Raven Hill Formation p3, and said to overlie Plumbago Formation.||Saltbush Group|Includes Black Maria Formation, Oonartra Creek Formation|Correlated with Purnamoota Subgroup, Overlies Plumbago Formation, Ethiudna Subgroup, overlain by Walparuta Formation||19-DEC-21
72575|Raven Hill Subgroup|63866|5|Briefly described|p41||||||||Pelite and psammopelite with minor psammite layers. Locally graphitic and contains calc-silicate ellipsoids and well-laminated sanguiferous banded iron formations.|
72575|Raven Hill Subgroup|64741|5|Briefly described|p301 Fig. 4, p309|Paleoproterozoic|Paleoproterozoic|Of Saltbush Group. Includes Black Maria and Oonartra Creek Formations. Geological province: Olary Domain. Equivalent of Purnamoota Subgroup in Broken Hill Domain.||||||07-FEB-11
72575|Raven Hill Subgroup|64944|5|Briefly described|p28 Fig. 1, p29 Tb. 1|Paleoproterozoic|Paleoproterozoic|Of Saltbush Group. Geological province: Olary Domain.||||||07-FEB-11
72575|Raven Hill Subgroup|66302|5|Briefly described|p36 Fig.9, p38, p39|Statherian|Statherian|Olary Domain, Curnamona Province. ||Saltbush Group|Includes the Black Maria Formation, Oonartra Creek Formation.||Siliciclastic metasedimentary rocks, mainly sandstone with thick mudstone intervals. Contains calc-silicate ellipsoids and well-laminated, banded iron formations.|
72575|Raven Hill Subgroup|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Olary Domain.||Saltbush Group.||||
72575|Raven Hill Subgroup|70405|4|Described|p28, p41|Paleoproterozoic|Paleoproterozoic||1685 Ma - 1693 Ma|Saltbush Group|Includes Black Maria Formation, Oonartra Creek Formation|Intruded by Lady Louise Suite, correlated with Purnamoota Subgroup|Pelite dominated succession with fine-medium grained psammite interbeds that show sparse grading. Calc silicate ellipsoids common throughout.|
72575|Raven Hill Subgroup|70657|4|Described|p13 Fig.6, p14-15, p17, p20, p34, p40-41|Statherian|Statherian|See also p64, p66. Curnamona Province, Olary Domain. Fig.6 suggests it is part of Broken Hill Group. Mineralisation described.|<1693 +/- 3 Ma - >1685 Ma|Saltbush Group|Includes Black Maria Formation and Oonartra Creek Formation.|Overlies Plumbago Formation (Larry Macs Subgroup). Underlies Walparuta Formation. Equivalent to Purnamoota Subgroup (Broken Hill Group).||
72575|Raven Hill Subgroup|70658|5|Briefly described|p3, 7, 15|Paleoproterozoic|Paleoproterozoic|Olary Domain, Curnamona Province.||Saltbush Group.|Black Maria, Oonartra Creek Formations.|Equivalent to upper part of Broken Hill Group.||
72575|Raven Hill Subgroup|73429|5|Briefly described|p106 Fig.2, p107|Statherian|Statherian|Curnamona Province, Olary Domain.||Saltbush Group||Overlies Larry Macs Subgroup, underlies Walparuta Subgroup||
25432|Rawnsley Quartzite|7931|5|Briefly described|p97, p99 Fig. 2|Ediacaran|Ediacaran|Of the Pound Subgroup. Contains the well-known Ediacara fossils assemblage within the Ediacara Member.||||||07-FEB-11
25432|Rawnsley Quartzite|22646|6|Mentioned|Fig 4 on p 102|Neoproterozoic|Neoproterozoic|Adelaide Geosyncline (West).  Parent -  Pound Subgroup.  Age - Ediacarian in text.||||||
25432|Rawnsley Quartzite|22688|6|Mentioned|127|||||||||
25432|Rawnsley Quartzite|22921|6|Mentioned|37|||||||||
25432|Rawnsley Quartzite|22927|5|Briefly described|41|||Geol province Adelaide Geosyncline||||||
25432|Rawnsley Quartzite|23211|6|Mentioned|Fig.2|||of Pound Subgroup.||||||
25432|Rawnsley Quartzite|23250|5|Briefly described|p1124 Fig.2||Neoproterozoic III|Of Wilpena Group.Correlate of Arumbera Sandstone.||||||20-JAN-09
25432|Rawnsley Quartzite|23282|6|Mentioned|p94|||||||||
25432|Rawnsley Quartzite|23287|6|Mentioned|Fig.2-4|||Age: Upper Ediacarian. of Pound Subgroup, Adelaide Geosyncline.||||||
25432|Rawnsley Quartzite|23401|6|Mentioned|p573|||||||||
25432|Rawnsley Quartzite|23913|4|Described|p110 Fig. 2|Adelaidean|Adelaidean|Geological Province: Central Flinders Zone.  Of the Wilpena Group. Underlain by Bonney Sandstone.||||||22-NOV-06
25432|Rawnsley Quartzite|23981|5|Briefly described|p10 Fig. 5, p52 Fig. 20|Precambrian|Precambrian|Geological Province: Arowie Basin.||||||
25432|Rawnsley Quartzite|24195|5|Briefly described|p48|Precambrian|Precambrian|Geological Province: Adelaide Geosyncline||||||
25432|Rawnsley Quartzite|24281|5|Briefly described|p7|Neoproterozoic|Neoproterozoic|||||||
25432|Rawnsley Quartzite|24476|4|Described|p547 Fig. 4|Vendian|Vendian|Overlies the Bonney Sandstone.  Geological Province: Adelaide Fold Belt.||||||03-MAY-13
25432|Rawnsley Quartzite|24484|4|Described|p803 Fig. 3. p804|Neoproterozoic|Neoproterozoic|Of the Wilpena Group. Overlies the Bonney Sandstone. Disconformably overlain by the Uratanna Formation.||||||
25432|Rawnsley Quartzite|24546|5|Briefly described|p2 - 3 Fig.2|Neoproterozoic|Neoproterozoic|Of Wilpena Group. Geological Province: Adelaide Fold Belt.||||||16-JAN-08
25432|Rawnsley Quartzite|24586|5|Briefly described|p51 Fig. 1|Adelaidean|Adelaidean|Of the Pound Subgroup (Wilpena Group, Heysen Supergroup). Geological Province: Adelaide Geosyncline.||||||
25432|Rawnsley Quartzite|30220|6|Mentioned|p213|||||||||
25432|Rawnsley Quartzite|30374|6|Mentioned|Fig.5|||Correlation. Upper Precambrian age.||||||
25432|Rawnsley Quartzite|37015|6|Mentioned|Fig.2|||||||||
25432|Rawnsley Quartzite|37627|6|Mentioned|p185|||||||||
25432|Rawnsley Quartzite|38157|6|Mentioned|Table V|||See also p269.||||||23-JAN-19
25432|Rawnsley Quartzite|38970|6|Mentioned|p105|||Upgrade of Rawnsley Quartzite Member by Jenkins (1975)||||||
25432|Rawnsley Quartzite|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Marinoan||||||
25432|Rawnsley Quartzite|40537|6|Mentioned|p328|||||||||
25432|Rawnsley Quartzite|41001|6|Mentioned|p169|||||||||
25432|Rawnsley Quartzite|41236|5|Briefly described|p63|||||||||
25432|Rawnsley Quartzite|41424|5|Briefly described|p299|||||||||
25432|Rawnsley Quartzite|41429|3|Fully described|p243|||||||||
25432|Rawnsley Quartzite|41496|6|Mentioned|p52|||||||||
25432|Rawnsley Quartzite|41794|6|Mentioned|Fig.2|||||||||
25432|Rawnsley Quartzite|41801|6|Mentioned|p219|||||||||
25432|Rawnsley Quartzite|42095|5|Briefly described|Fig.3 P31|||||||||
25432|Rawnsley Quartzite|42098|5|Briefly described|Table 2 P54|||||||||
25432|Rawnsley Quartzite|42213|5|Briefly described|p471|||See also Fig.2||||||
25432|Rawnsley Quartzite|42222|6|Mentioned|p20|||||||||
25432|Rawnsley Quartzite|42233|6|Mentioned|p249|||||||||
25432|Rawnsley Quartzite|42240|6|Mentioned|Fig.2 P165|||||||||
25432|Rawnsley Quartzite|42241|6|Mentioned|p179|||||||||
25432|Rawnsley Quartzite|42433|6|Mentioned|p178|||||||||
25432|Rawnsley Quartzite|42643|6|Mentioned|p25|||||||||
25432|Rawnsley Quartzite|43052|5|Briefly described|p194,Table 6.1|||of Pound Subgroup||||||
25432|Rawnsley Quartzite|43595|6|Mentioned|p548|||||||||
25432|Rawnsley Quartzite|43622|6|Mentioned|p38|Neoproterozoic||||||||
25432|Rawnsley Quartzite|43650|6|Mentioned|Fig.2,p444|||||||||
25432|Rawnsley Quartzite|43845|5|Briefly described|Fig3 p43||Neoproterozoic|In Wilpena Group||||||12-JUL-16
25432|Rawnsley Quartzite|44133|5|Briefly described|p20, 22|||Overlain disconformably by Uratanna Formation, Parachilna Formation.||||||
25432|Rawnsley Quartzite|60889|5|Briefly described|p245 Fig.2, p248-50|Neoproterozoic|Neoproterozoic|Age: late Neoproterozoic. Ediacara fauna-bearing. Submarine channels occur at base. Relationships continued: Where both Uratanna Formation and Parachilna Formation are missing, is overlain by younger carbonates (Woodendinna Dolomite and lower Wilkawillina Limestone). Arrowie Basin.|~550 Ma.|||Interleaves with Billy Springs Formation. Is overlain unconformably by Uratanna Formation or, where absent, disconformably by Parachilna Formation. Continued in Comments.||21-SEP-17
25432|Rawnsley Quartzite|60959|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Of the Pound Subgroup. Mature, medium grained sandstone with intervals of trough cross bedding and wavy lamination.||||||
25432|Rawnsley Quartzite|61236|5|Briefly described|p22, p24 Fig. 1|Adelaidean|Adelaidean|Sandstone beds with fossil impressions.||||||14-MAY-07
25432|Rawnsley Quartzite|61308|5|Briefly described|p7|Proterozoic|Proterozoic|||||||30-JUN-06
25432|Rawnsley Quartzite|61565|5|Briefly described|p609 Fig. 3|Neoproterozoic III|Neoproterozoic III|Geological Province: Adelaide Fold Belt.||||||20-APR-06
25432|Rawnsley Quartzite|61732|5|Briefly described|p4, p28 Fig. 13|Marinoan|Marinoan|Of the Pound Subgroup (Wilpena Group). Includes the Ediacara and Patsy Hill Members. Geological Province: Adelaide Rift Complex.||||||07-FEB-11
25432|Rawnsley Quartzite|62085|6|Mentioned|p20 fig 5|Ediacaran|Ediacaran|Northern Ediacara Range.||Unit in Pound Subgroup.|Includes Ediacara Member.|||
25432|Rawnsley Quartzite|62592|5|Briefly described|p50 Table 5.1.|Ediacaran|Ediacaran|Adelaide Geosyncline.||Unit in Wilpena Group.||Overlies Bonney Sandstone.|White orthoquartzite.|
25432|Rawnsley Quartzite|63397|6|Mentioned|p15|||||||||
25432|Rawnsley Quartzite|64455|5|Briefly described|p138 Fig. 1|Early Cambrian|Early Cambrian|Of Pound Subgroup. Includes Ediacara Member and Chase Quartzite Member. Horizontal burrows. White Quartzite.||||||29-JAN-09
25432|Rawnsley Quartzite|64460|5|Briefly described|p195, p197, p198, p199|||Of Pound Subgroup. Includes Ediacara Member and Chase Quartzite Member. White sandstones or quartzites.||||||
25432|Rawnsley Quartzite|64801|6|Mentioned|p111|Neoproterozoic|Neoproterozoic||||Includes Ediacara Member.|||23-JAN-19
25432|Rawnsley Quartzite|64829|5|Briefly described|p1085|Ediacaran|Ediacaran|Palaeotopography developed on this unit is disconformably onlapped by either the Parachilna or Uratanna Formations. Unit discussed in the context of soilscapes and palaeosols.||||||07-FEB-11
25432|Rawnsley Quartzite|65686|5|Briefly described|p420,  p409 Fig 2|Ediacaran|Ediacaran|Arrowie Basin/Flinders Ranges.||||Underlies the Uratanna Formation.||07-MAY-12
25432|Rawnsley Quartzite|65892|4|Described|p7 Fig.3, p8, p16, p26-28, p32-34|Ediacaran|Ediacaran|See also p38-39, p41 Fig.23. Flinders Ranges. Contains Ediacara fauna. Mainly tidal to storm wave base sandstones.|c.550 Ma.|Unit in Wilpena Group.|Includes Ediacara Member.|Is overlain locally by Parachilna Formation or disconformably by Uratanna Formation.|White to pale yellow and pinkish grey quartzite and quartz sandstone.|
25432|Rawnsley Quartzite|65925|5|Briefly described|Appendix 2.||||||||Quartzite and sandstone, white or light grey, locally flaggy and fossiliferous.|
25432|Rawnsley Quartzite|66569|5|Briefly described|p860, p861 fig.2,|Ediacaran|Ediacaran|Of Wilpena Group; shallow marine and estuarine sediments; contains Ediacara Member; unconformably underlies Uratanna Formation; overlies Bonney Sandstone.||||||
25432|Rawnsley Quartzite|67030|6|Mentioned|p409,  Fig. 2|Ediacaran|Ediacaran|Maximum age inferred from underlying Bonney Sandstone age.|< 556 +/- 24 Ma|||Overlies the Bonney Sandstone.||26-APR-12
25432|Rawnsley Quartzite|67344|6|Mentioned|p259|Late Ediacaran|Late Ediacaran|Contains exceptionally well-preserved fauna.||||||
25432|Rawnsley Quartzite|67484|5|Briefly described|p294 Tb.1|Ediacaran|Ediacaran|Adelaide Rift Complex.||Of the Pound Subgroup.|Includes Chace Quartzite Member and Ediacara Member.|Overlain by the Hawker Group. Underlain by Bonney Sandstone.||
25432|Rawnsley Quartzite|67620|5|Briefly described|p5, 22|Ediacaran|Ediacaran|Adelaide Rift Complex. Shallow-marine deposits; contains petee ridges and dimpled surface structures (microbial mats).||Pound Subgroup.|Ediacara, Chace Quartzite, Members.|Overlies Bonney Sandstone. Is overlain by Hawker Group.||
25432|Rawnsley Quartzite|68030|4|Described|p239, p241-243|Cambrian|Ediacaran|Flinders Ranges. Shallow marine, wave and tide reworked deltaic succession marking a phase of uplift and erosion on the Gawler Craton (Gehling, 2000) and onset of Petermann Orogeny 600 km to the NW between the Officer and Amadeus basins (Fl¿ttmann et al., 2004). The light colour and indurated ridges and outcrops are likely remnants of early Cenozoic leaching and surface silicification. Can be subdivided into multiple facies and parasequences (see p240-241). See p241-243 for in depth discussion of Ediacaran biota.|||Includes upper Rawnsley Quartzite and Ediacara Member.||Pale, medium to coarse grained, felspathic sandstone. Commonly reddish with Fe-stained grains within incised sections.|26-JUN-19
25432|Rawnsley Quartzite|68138|5|Briefly described|p156|Neoproterozoic|Neoproterozoic|Adelaide Rift Complex.||Pound Subgroup.|Ediacara, Chace Quartzite, Members.|||
25432|Rawnsley Quartzite|68269|6|Mentioned|p674|||Adelaide Geosyncline.||Wilpena Group|Ediacara Member|Underlain by Bonney Sandstone. Unconformably overlain by Uratanna Formation.|Sandstone dominated.|
25432|Rawnsley Quartzite|68271|5|Briefly described|p693-695|||Adelaide Rift Complex.|||Includes Ediacara Member.|Underlain by Billy Springs Formation.|White feldpsathic quartzite.|
25432|Rawnsley Quartzite|68473|6|Mentioned|p531|Ediacaran|Ediacaran|||||Equivalent to the Flat Rock Formation.||
25432|Rawnsley Quartzite|68735|5|Briefly described|p233, p234|Ediacaran|Ediacaran|||||Overlain by the Uratanna Formation. Disconformably overlain by the Parachilna Formation.||
25432|Rawnsley Quartzite|69019|6|Mentioned|p61.|Neoproterozoic|Neoproterozoic|Mawson's (1938) informal subdivision of his Pound Quartzite into a lower red sandstone member and an upper white quartzite member was formalised by Forbes (1971) who defined them as Bonney Sandstone Member and Rawnsley Quartzite Member respectively. These were later (Jenkins, 1975) elevated to Formation status (within the Pound Subgroup).||||||
25432|Rawnsley Quartzite|70031|5|Briefly described|p245|Ediacaran|Ediacaran|Adelaide Geosyncline. ||Unit of Pound Subgroup.||Upper unit of Pound Subgroup. Underlain by Bonney Sandstone.||
25432|Rawnsley Quartzite|70082|6|Mentioned|p2|Ediacaran|Ediacaran|Flinders Ranges. Contains red beds and periglacial paleosols.||||||
25432|Rawnsley Quartzite|70334|5|Briefly described|p78|Ediacaran|Ediacaran|Geological province: Gawler Craton. Of Adelaide Geosyncline. Prograding shore face, barrier and tidal channel complex deposited after renewed marine transgression. Undewent submarine channel incision, and subsequently infilled by turbiditic sands and silts of the Ediacara Member.  Completely eroded from the Flinders Ranges during Cambrian uplift.||Unit of Pound Subgroup.||||
25432|Rawnsley Quartzite|70384|5|Briefly described|Map legend.|Ediacaran|Neoproterozoic|Adelaide Geosyncline.||Of Pound Subgroup.|Includes Ediacara Member.|Equivalent to Billy Springs Formation.|White or light grey, locally flaggy, quartzite and sandstone.|23-JAN-19
25432|Rawnsley Quartzite|70407|6|Mentioned|p112|||||Of Pound Subgroup|Includes Ediacara Member.|||
25432|Rawnsley Quartzite|70790|5|Briefly described|p257-260, p266, p268, p270|Ediacaran|Ediacaran|Adelaide Rift Complex. Hosts the Ediacaran metazoan fossil assemblage. Deposition in a variety of shallow-marine and intertidal environments.||Of Wilpena Group.|Includes Chace Member, Ediacara Member.|Overlies Bonney Sandstone.||23-JAN-19
25432|Rawnsley Quartzite|70833|5|Briefly described|p184|Ediacaran|Ediacaran|Of Arrowie Basin. ||||Overlain disconformably by Uratanna Formation or Parachilna Formation.||
25432|Rawnsley Quartzite|71080|6|Mentioned|p21|||South Australia.|||Includes Ediacara Member.|||
25432|Rawnsley Quartzite|71250|5|Briefly described|p69-70|Ediacaran|Ediacaran|Central Flinders Ranges. A shallow-marine, deltaic succession.||Pound Subgroup.|Chace Quartzite Member, Ediacara Member.|Disconformably overlies Bonney Sandstone.|Clean feldspathic sandstones.|
25432|Rawnsley Quartzite|72449|5|Briefly described|p1, p2 Map Legend|Neoproterozoic|Neoproterozoic|Shallow marine and possibly fluvial environment. Shown in image on p1, 'Ripple marks in the Rawnsley Quartzite, Wilpena Pound, looking towards Chace Range'. (Courtesy of Bernd Stoecker; photo 044287). Dickinsonia costata in the Ediacara Member, Rawnsley Quartzite, Brachina Gorge (x 0.7). (Photo 042162)|||Includes Ediacara Member.|Overlies Bonney Sandstone.|White, medium to coarse grained cross-bedded quartzite with lenticular beds. Lower half includes the Ediacara Member, comprising siltstone, fossil bearing sandstone grading up into white cross-bedded quartzite.|
25432|Rawnsley Quartzite|72451|6|Mentioned|p4 Fig. 1|Late Proterozoic|Late Proterozoic|Adelaidean age. Appears only in Figure 1.||||||
25432|Rawnsley Quartzite|73086|6|Mentioned|p85|Ediacaran|Ediacaran|Exhibits 'textured organic surfaces (TOS)' relating to microbially derived films that may form under high-energy conditions (Gehling and Droser, 2009).||||||
25432|Rawnsley Quartzite|73222|6|Mentioned|p6, p11, p16, p23-24|Ediacaran|Ediacaran|Adelaide Rift Complex.||Pound Subgroup, Wilpena Group, Heysen Supergroup||||
25432|Rawnsley Quartzite|73236|6|Mentioned|p40|||Flinders Ranges.||Wilpena Group, Heysen Supergroup||||
25432|Rawnsley Quartzite|73255|6|Mentioned|p534 Fig.2|Ediacaran|Ediacaran|||||Overlies the Ediacara Member, underlies the Uratanna Formation.||
25432|Rawnsley Quartzite|74367|5|Briefly described|p7 Fig.6, p8-9, p11, p16-17, p20, p22-23|Ediacaran|Ediacaran|See also p14.|570+/-23 Ma LA-ICP-MS detrital zircon MDA|Pound Subgroup||||
24469|Recovery Formation|22772|5|Briefly described|Table13.1|Cryogenian|Cryogenian|||||||
24469|Recovery Formation|22857|5|Briefly described|Tb. 13.1 (insert p70-71)|Willouran|Willouran|Of the Curdimurka Subgroup (Callanna Group).||||||
24469|Recovery Formation|24175|4|Described|p9|Neoproterozoic|Neoproterozoic|Of Curdimurka Subgroup. Overlies Dunns Mine Limestone. Max. thickness: 2217m.||||||13-FEB-08
24469|Recovery Formation|24321|5|Briefly described|Map legend|Adelaidean|Adelaidean|Parent: Curdimurka Subgroup.||||||13-FEB-08
24469|Recovery Formation|37854|2|Defined|p11|Adelaidean|Adelaidean|Prob.Late Willouran||||||
24469|Recovery Formation|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Willouran.||||||13-FEB-08
24469|Recovery Formation|40294|6|Mentioned|p9|||||||||
24469|Recovery Formation|41402|6|Mentioned|p42|||||||||
24469|Recovery Formation|41403|4|Described|p62|||||||||
24469|Recovery Formation|41404|6|Mentioned|p73|||||||||
24469|Recovery Formation|42087|5|Briefly described|Fig.2 P15|||||||||
24469|Recovery Formation|42222|5|Briefly described|p12|||||||||
24469|Recovery Formation|42238|5|Briefly described|Table 1 P75|||||||||
24469|Recovery Formation|43052|5|Briefly described|p175,Table 6.1|||Of Curdimurka Subgroup.||||||13-FEB-08
24469|Recovery Formation|60718|5|Briefly described|p49 Fig. 2, P50, 52|Adelaidean|Adelaidean|Thickness varies from in type section: 2200m to 100m near Dunns Mine. Geological Province: Adelaide Geosyncline.||Of Curdimurka Subgroup (Callanna Group).||Unconformably underlies Hogan Dolomite.||15-APR-11
24469|Recovery Formation|64796|6|Mentioned|p190 Fig.8, p194 Tb.2, p200 Fig.10|Neoproterozoic|Neoproterozoic|||Unit in Curdimurka Subgroup.||Overlies Dunns Mine Limestone. Is overlain by Hogan Dolomite.||
24469|Recovery Formation|64797|6|Mentioned|p161 Tb.4|||Adelaide Rift Complex. Lithology/rank not shown on diagram. S-isotope data. ||||||
24469|Recovery Formation|69019|5|Briefly described|p37.|Neoproterozoic|Neoproterozoic|Defined by Murrell (1977) with 5 un-named members. Type section 3 km SE of Dome Hill. Cyclic siltstone and sandstone sequences. Thickness of 2,217 m to the west.||Unit in Curdimurka Subgroup.|||Siltstone: dark grey, thinly bedded to laminated, micaceous, with mudcracks; sandstone: grey, flaggy, with halite and/or gypsum casts; minor dolomite; rare domal stromatolites.|
24469|Recovery Formation|72456|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Marree 1:250k map sheet. |||||Siltstone, grey, thin bedded, micaceous; sandstone with halite casts.|
24469|Recovery Formation|72492|5|Briefly described|p2 Fig.1, p5 Fig.4c and d|Neoproterozoic|Neoproterozoic|In Willouran Ranges. Siltstone slabs may exhibit wave ripples.||Curdimurka Subgroup||Overlies Dunns Mine Limestone and underlies Hogan Dolomite.|Includes stromatolites, siltstone with desiccation cracks and ripples.|
24469|Recovery Formation|73222|6|Mentioned|p7|Tonian|Tonian|Willouran Ranges. Torrensian.||Curdimurka Subgroup, Callanna Group, Warrina Supergroup||Unconformably underlain by Dunns Mine Limestone. Overlain by Hogan Dolomite. Possibly equivalent to Niggly Gap Beds.||
24469|Recovery Formation|74367|6|Mentioned|p7 Fig.6, p9, p12-14, p20|||||Curdimurka Subgroup||||
82231|Red Banks Charnockite|73026|4|Described|p24|||Type section occurs at Red Banks immediately west of Cape Carnot. Crops out along the Whalers Way coastline. SHRIMP zircon analyses give two ages, 1722 +/- 7 Ma and 2011 +/- 7 Ma [it is unclear what these ages mean from the text].|||||Charnockitic orthogneiss.|05-AUG-21
82231|Red Banks Charnockite|73027|5|Briefly described|p29-30, p32, p38|Statherian|Orosirian|Red Banks is the type location for this unit. Crops out along the Whalers Way coastline.SHRIMP U-Pb zircon analyses obtained from the charnockite give two ages. Finely oscillatory zoned grains typical magmatic zircon give an age of 2011 +/-7 Ma. New zircon that occurs as variably thick (up to 80 mm) mantles on magmatic cores and less commonly as individual crystals give an age of 1722 +/- 7 Ma (Jagodzinski et al., 2012).||||Intrudes the Carnot Gneiss.|K-feldspar-orthopyroxene-quartz-plagioclase-biotite-garnet bearing orthogneiss.|05-AUG-21
82231|Red Banks Charnockite|73122|5|Briefly described|p22, 29|||Cape Carnot. Metamorphosed at 1722 +/- 7 Ma. Appears as Redbanks Charnockite on p22.|2011 +/- 7 Ma (magmatic age).||||Orthogneiss after charnockite.|
79904|Red Conglomerate Member|66302|6|Mentioned|p47|Statherian|Statherian|Ages are U-Pb dates from McAveney and Reid (2008).|1765 +/- 15 to 1746 +/- 9 Ma |Corunna Conglomerate||||
79904|Red Conglomerate Member|71235|5|Briefly described|p8, p11, p14-p16, p22|||Zircon characteristics, sampling location and U-Pb analyses are discussed for numerous dated samples.|1746 +/- 9 Ma (Max dep age)|Corunna Conglomerate|||Poorly bedded conglomerate.|
82474|Red Dam dacite porphyry|72949|6|Mentioned|p36|Calymmian|Calymmian|Olympic Domain, north. Olympic Dam / Punt Hill area. May be a part of Olympic Dam Granite.|1594 +/- 0.4 Ma|||||
80480|Refuge Rocks granite|63866|5|Briefly described|p19|Statherian|Statherian|Cleve Domain, Gawler Craton.|c. 1740-1730 Ma (Fanning et al., 2007)|Donington Suite||||
26322|Relief Sandstone|22613|4|Described|p16|Neoproterozoic|Neoproterozoic|Officer Basin||||||
26322|Relief Sandstone|22614|5|Briefly described|map|Cambrian|Cambrian|||||||
26322|Relief Sandstone|22746|5|Briefly described|Fig.3 p515|Early Cambrian|Early Cambrian|||||||
26322|Relief Sandstone|22922|6|Mentioned|34|||Overlying unit Observatory Hill Formation||||||
26322|Relief Sandstone|23054|6|Mentioned|p17,36||Early Cambrian|||||||
26322|Relief Sandstone|23282|2|Defined|p68||Early Cambrian|of Brewer et al (1987). Age: Early Cambrian 540 - 524Ma. of Marla Group, Officer Basin.||||||
26322|Relief Sandstone|23287|6|Mentioned|Fig.4|||Age: Lower Cambrian. of Eastern Officer Basin.||||||
26322|Relief Sandstone|23288|6|Mentioned|Fig.5||Early Cambrian|||||||
26322|Relief Sandstone|23524|5|Briefly described|p221 Fig. 3|Early Cambrian|Early Cambrian|||||||
26322|Relief Sandstone|23981|5|Briefly described|p10 Fig. 5|Tommotian|Tommotian|Geological Province: eastern Officer Basin.||||||26-FEB-07
26322|Relief Sandstone|24112|5|Briefly described|p254 Fig.2, p257 Tb.1|Early Cambrian|Early Cambrian|Geological Province: Officer Basin||||||
26322|Relief Sandstone|40945|2|Defined|p10|Early Cambrian|Early Cambrian|||||||
26322|Relief Sandstone|42065|4|Described|p186|||See also Fig.3||||||
26322|Relief Sandstone|42095|5|Briefly described|Fig.3 P31|||||||||
26322|Relief Sandstone|42096|6|Mentioned|p36|||||||||
26322|Relief Sandstone|42816|4|Described|p14|||||||||
26322|Relief Sandstone|43052|5|Briefly described|Table 2.1|||||||||
26322|Relief Sandstone|43650|6|Mentioned|Fig.2,p444|||||||||
26322|Relief Sandstone|43657|6|Mentioned|Fig.3,p4||Cambrian|||||||
26322|Relief Sandstone|43690|6|Mentioned|Fig.2,p157||Cambrian|||||||
26322|Relief Sandstone|43732|6|Mentioned|p3||Early Cambrian|||||||
26322|Relief Sandstone|43743|6|Mentioned|Fig.2,p33||Early Cambrian|||||||
26322|Relief Sandstone|44109|5|Briefly described|p22 Fig. 19|Cambrian|Cambrian|Of the Marla Group. Geological Province: central Officer Basin.||||||
26322|Relief Sandstone|44133|4|Described|p4 Fig. 7.2, 9 Fig. 7.5, 35|Early Cambrian|Early Cambrian|Geological Province: Eastern Officer Basin. Of the Marla Group. Overlain conformably by Ouldburra Formation. Thickness: 79m+.||||||
26322|Relief Sandstone|44289|5|Briefly described|Map Legend||Early Cambrian|||||||
26322|Relief Sandstone|44695|5|Briefly described|Map Legend||Cambrian|||||||
26322|Relief Sandstone|60565|5|Briefly described|p18, p20 Fig. 3b|Cambrian|Cambrian|Fluvial. Overlies the Rodda beds.||||||
26322|Relief Sandstone|61732|6|Mentioned|p60, p67, p73|Cambrian|Cambrian|Of the Marla Group. Unconformably overlies Murnaroo Formation.||||||07-FEB-11
26322|Relief Sandstone|62570|5|Briefly described|p579, p580 Figs. 2 and 3|Early Cambrian|Early Cambrian|Base of Marla Gp. Unconformable over Ungoolya Group. Contains hematitic sst and siltst., which pass transitionally into salt, limest., dolostone, siltst. and sst. Salt is thin, brown and hematitic and often interbedded with red-brown silty dolostone.||||||
26322|Relief Sandstone|64794|6|Mentioned|p238 fig 2|Early Cambrian|Early Cambrian|||||||
26322|Relief Sandstone|64797|6|Mentioned|p153 Fig.2|Ediacaran|Ediacaran|Officer Basin. Lithology/rank not shown on diagram.||||||
26322|Relief Sandstone|65410|6|Mentioned|p74.|||Officer Basin. Probably part of Supersequence 4.||||||
26322|Relief Sandstone|65416|6|Mentioned|p146.|||Sequence LP4A. Suggested by Perincek (1996) to post-date the Petermann Ranges Orogeny.||||||
26322|Relief Sandstone|67120|5|Briefly described|Map legend|Cambrian|Cambrian|||Marla Group|||Sandstone, planar cross-bedded, fine to medium-grained, aeolian; sandstone with mud drapes, mud-chip intra clasts, scoured, fluviatile.|
26322|Relief Sandstone|67536|6|Mentioned|Map Legend|||One of several Formations mapped collectively as Em4.|||||Aeolian, fluvial and evaporitic to tidal sandstone to mudstone; marine limestone and dolomite.|
26322|Relief Sandstone|69648|4|Described|p19, map legend|Early Cambrian|Early Cambrian|Of Tallaringa Trough. Unit occurs in drillholes on adjacent map sheets and may extend into subsurface of northeastern OOLDEA.||Marla Group||Passes transitionally up into Ouldburra Formation.|Sediments.|
26322|Relief Sandstone|69946|6|Mentioned|p38|||||||Unconformably overlies Ungoolya Group. Is overlain conformably by Ouldburra and Cootanoorina Formations.||
26322|Relief Sandstone|70336|5|Briefly described|Map legend|Cambrian|Cambrian|||Of Marla Group.|||Planar cross-bedded, fine- to medium-grained aeolian sandstone; scoured, fluviatile sandstone with mud drapes, mud-chip intraclasts.|12-JAN-16
26322|Relief Sandstone|70833|5|Briefly described|p203|Cambrian|Cambrian|Of Officer Basin. Coeval with Ouldburra Formation; broadly coincident with Hawker Group.||||||
26322|Relief Sandstone|71342|6|Mentioned|Ch5 p38|Cambrian|Cambrian|||||Unconformably overlies the Ungoolya Group. Overlain by the Ouldburra Formation.||
26322|Relief Sandstone|72478|6|Mentioned|p8|Early Cambrian|Early Cambrian|Officer Basin.|c. 536-524 Ma|Marla Group||||25-MAR-21
26322|Relief Sandstone|73099|5|Briefly described|Map legend.|Middle Cambrian|Early Cambrian|Officer Basin.||Marla Group.||Overlies Narana Formation (Ungoolya Group). Is overlain by Observatory Hill Fomation.|Pale grey to red-brown, fine- to very coarse-grained quartz and feldspathic quartz sandstone with thin interbeds of grey to red-brown siltstone and claystone.|
29853|Remarkable Granite|64282|5|Briefly described|Map legend|Middle Cambrian|Middle Cambrian|Part of Delamerian Orogeny.  Medium-grained, grey, equigranular biotite granite, minor metasedimentary xenoliths.||||||23-JUN-08
29853|Remarkable Granite|73107|5|Briefly described|Map legend.|Middle Cambrian|Middle Cambrian|Delamerian Orogeny.|||||Medium-grained, grey, equigranular biotite granite, minor metasedimentary xenoliths.|
39161|Renowden Metabasalt Member|24475|2|Defined|p55|Paleoproterozoic|Paleoproterozoic|Of Matta Formation. Originally defined as Renowden Metabasalt by Zang (2002).||||||07-NOV-08
39161|Renowden Metabasalt Member|60958|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Matta Formation. Fine-grained, massive, foliated basalt. Intrudes Wardang Volcanics. Age: ~1750Ma. Geological Province: Gawler Craton.||||||07-NOV-08
39161|Renowden Metabasalt Member|61121|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Matta Formation. Fine-grained, massive, foliated basalt with hornblende, plagioclase, clinopyroxene and biotite; quartz-rich vesicles suggest a formerly scoriaceous texture. Intrudes Wardang Volcs.  Age: ~1750Ma.Geological Province: Gawler Craton.||||||07-NOV-08
39161|Renowden Metabasalt Member|65375|5|Briefly described|p19, p23.|||Fine-grained extrusive and shallow intrusive.||Unit in Matta Formation.||Intrudes metasediments of Aagot Member and Wardang Volcanics.|Fine-grained amphibolite or metabasalt; anhedral to subhedral crystals of hornblende and plagioclase, with biotite; occasional chlorite, sphene, opaques, quartz, apatite and rutile as accessories.|
39161|Renowden Metabasalt Member|65376|6|Mentioned|p101 Fig.3.1.|||||||||
39161|Renowden Metabasalt Member|73092|6|Mentioned|p3, p23, p26|||Yielded a metamporphic age of 1547 +/- 56 Ma. Dated sample is metabasalt from Port Victoria.||Wallaroo Group|||Massive to foliated metabasalt.|
39161|Renowden Metabasalt Member|73493|5|Briefly described|p727|||Metamorphosed at 1547+/-56 Ma (Reid, Zhao et al., 2020).||Wallaroo Group||||
78839|River Broughton beds|64793|6|Mentioned|p285 fig 4|||Adelaide Rift Complex. Fig. 4 Range chart of stromatolite distributions in the Centralian Superbasin and Adelaide Rift Complex. ?Parmites f. indet. (in Preiss 1987)||Unit in Callanna Group.||||
78839|River Broughton beds|64797|6|Mentioned|p158, p161 Tb.4|||S-isotope data. Authors say that it is uncertain whether this unit belongs to Callanna or Burra Group, but is included in Callanna Group because of carbon isotope results (Hill, 1998).||Callanna Group.||||
34745|River Wakefield Formation|22889|4|Described|p33-34 & p38|Adelaidean|Adelaidean|The River Wakefield Formation is part of the now obsolete River Wakefield Subgroup, some units within the sucession have changed, details in text.  Location of reference section advised p38.||||||
34745|River Wakefield Formation|62724|5|Briefly described|p16, p17 Fig. 4|Torrensian|Torrensian|Of the Emeroo Subgp (Burra Gp). Immature fine-grained sandstone and siltstone, commonly flaser-bedded, with persistent basal conglomerate and thinner conglomerate and sandstone lenses higher up. Conformably overlain by Skillogalee Dolomite.||||||07-FEB-11
34745|River Wakefield Formation|65925|5|Briefly described|Appendix 2.||||||||Dolomite; sandstone; siltstone; quartzite.|
34745|River Wakefield Formation|66109|6|Mentioned|p200|||||||||
34745|River Wakefield Formation|68207|6|Mentioned|p766, 768-769|||Mentioned in a graph showing Raman spectra of kerogen comprising Precambrian permineralised microfossils; demonstrating they are not merely graphite.|c.775 Ma.||||Contains Precambrian microfossils in chert.|
34745|River Wakefield Formation|70405|6|Mentioned|p51 table 4|Neoproterozoic|Neoproterozoic|||Emeroo Subgroup||||
34745|River Wakefield Formation|70819|6|Mentioned|p11, 13, 18-20|Neoproterozoic|Neoproterozoic|Western Clare Valley.||Emeroo Subgroup.||Overlies Blyth Dolomite.|Shallow-marine deposits: phyllitic slates and interbedded quartzite layers.|
34745|River Wakefield Formation|73110|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic||||||Dolomite; sandstone; siltstone; quartzite.|
34745|River Wakefield Formation|73188|6|Mentioned|p321-322|||Alma Fault scarp. Multiply deformed.|||||Highly schistose metasiltstone and quartzite.|
34745|River Wakefield Formation|74367|6|Mentioned|p7 Fig.6|||||Emeroo Subgroup||||
24623|Rockleigh Formation|39909|2|Defined|p3|late Pleistocene|late Pleistocene|||||||
24623|Rockleigh Formation|42499|5|Briefly described|Map legend|Pleistocene||||||||
26125|Rogue Formation|23768|5|Briefly described|p28 Fig.5|Oligocene|Eocene|Geological Province: St Vincent Basin.  See also p103, p123.||||||30-MAR-05
26125|Rogue Formation|29856|6|Mentioned|p37|||||||||
26125|Rogue Formation|30251|4|Described|p4|||Also mention P3.||||||
26125|Rogue Formation|30514|6|Mentioned|p103|||Upper Eocene age||||||
26125|Rogue Formation|30825|6|Mentioned|p32|||||||||
26125|Rogue Formation|32420|5|Briefly described|p149|||Large clay deposit. U.Eoc.- Oligoc?||||||
26125|Rogue Formation|32601|6|Mentioned|p677|||||||||
26125|Rogue Formation|33330|2|Defined|p160|Oligocene|late Eocene|Upper Eocene - Lower Oligocene||||||
26125|Rogue Formation|35689|6|Mentioned|Fig.33|||Stratigraphic correlation, St.Vincent Basin.||||||
26125|Rogue Formation|38699|6|Mentioned|p12|||||||||
26125|Rogue Formation|41513|6|Mentioned|p42|||||||||
26125|Rogue Formation|41626|6|Mentioned|Fig.2|||||||||
26125|Rogue Formation|42498|5|Briefly described|Map Legend|Eocene|Eocene|||||||
26125|Rogue Formation|42506|5|Briefly described|Map legend|Eocene||Age Tertiary||||||
26125|Rogue Formation|44133|5|Briefly described|p170, 165 Fig. 10.11|Late Oligocene|Late Eocene|Geological Province: Saint Vincent Basin. ||||||
26125|Rogue Formation|60958|5|Briefly described|Map Legend|Eocene|Eocene|Silty sandstone, calcareous sandstone, sandy siltstone and sandy limestone. Geological Province: Saint Vincent Basin.||||||
26125|Rogue Formation|61121|5|Briefly described|Map legend|Eocene|Eocene|Silty sandstone, calcareous sandstone, sandy siltstone and sandy limestone; abundant fossils including 'Spirocolpus (Turitella) aldingae'. Geological Province: St. Vincent Basin.||||||06-JUN-05
26125|Rogue Formation|61155|5|Briefly described|p3, p17|Early Oligocene|Late Eocene|Paralic sands. Overlies Throoka Silt in north of basin. Age: 37.5-31Ma. Geological Province: St Vincent Basin margins.||||||
26125|Rogue Formation|65375|4|Described|p34 Fig.7, pp35-36. |Paleogene|Paleogene|Lower part correlates with Blanche Point Formation. Described as Tertiary age but contains abundant and diverse Oligocene fossils, including numerous Spirocolpus aldingae. To 30 m thick in outcrop.|||Includes Port Julia Greensand Member|Unconformably overlies Throoka Silts, Muloowurtie Formation and Cape Jervis Formation. Grades into Aldinga Member of Port Willunga Formation.|Siliciclastic unit with silty sandstone, calcareous sandstone, sandy siltstone and sandy limestone. Uppermost part of sandstone contains abundant glauconite.|
26125|Rogue Formation|65891|6|Mentioned|p221 Fig.5. |Paleogene|Paleogene|Western St Vincent Basin. Priabonian age. ||||||
26125|Rogue Formation|67462|5|Briefly described|Map legend.||Eocene|Western Saint Vincent Basin.||||||
26125|Rogue Formation|68715|6|Mentioned|p31 Fig.5|Chattian|Bartonian|St Vincent Basin.|||Port Julia Greensand Member.|||07-APR-17
26125|Rogue Formation|70382|6|Mentioned|p28, p29 Fig 3, p30|Oligocene|Eocene|Geological province: Troubridge Basin.||||Conformably overlain by Port Vincent Limestone.|Sand, quartz; sandstone; siliceous sandstone; siliceous and sandy limestone; mudstone and clay; marine to marginal marine.|
26125|Rogue Formation|70660|6|Mentioned|p20|||||||Conformably overlies the Ruwarung Member.||
27299|Rook Tuff|22553|6|Mentioned|p77,p83|Cryogenian|Cryogenian|part of the Adelaidean sequence||||||
27299|Rook Tuff|22589|6|Mentioned|p129||Neoproterozoic|||||||
27299|Rook Tuff|22631|6|Mentioned|p177|Cryogenian|Cryogenian|||||||
27299|Rook Tuff|22772|4|Described|p65,Table13.1|Cryogenian|Cryogenian|Max Age: 802 (+/-) 10 Ma.||||||
27299|Rook Tuff|22857|5|Briefly described|p65, Tb. 13.1 (insert p70-71)|Willouran|Willouran|Of the Curdimurka Subgroup (Callanna Group). Age: 802+/-10Ma (Fanning, Ludwig et al, 1986). See also p399 App.1 Tb.A1.3.||||||
27299|Rook Tuff|22907|5|Briefly described|41|||Age 802 + - 10 Ma||||||
27299|Rook Tuff|23314|6|Mentioned|335|||||||||
27299|Rook Tuff|23557|5|Briefly described|p98|Cryogenian|Cryogenian|Age: 802+/-10Ma (U-Pb).||||||
27299|Rook Tuff|23562|5|Briefly described|p295 Fig 2|Cryogenian|Cryogenian|Age: 802+/-10 Ma||||||
27299|Rook Tuff|24175|4|Described|p9|Neoproterozoic III|Neoproterozoic|Of Curdimurka Subgroup.  Overlain by Dunns Mine Limestone; overlies Dome Sandstone.  Max. thickness: 60m.  Age: 802+/-10Ma (U-Pb zircon, Fanning et al, 1986).||||||
27299|Rook Tuff|24321|5|Briefly described|Map legend|Adelaidean|Adelaidean|Parent: Curdimurka Subgroup.  Age: 802+/-10Ma (Concordant U-Pb zircon)||||||
27299|Rook Tuff|24400|5|Briefly described|p155, p156|Neoproterozoic|Neoproterozoic|Of Callanna Group. Overlies Wooltana Volcanics. Age: 802+/-10Ma.||||||18-APR-13
27299|Rook Tuff|24401|5|Briefly described|p100|Neoproterozoic|Neoproterozoic|Age: 802+/-10Ma. Geological Province: Adelaide Geosyncline||||||03-MAR-05
27299|Rook Tuff|24604|5|Briefly described|p915|Neoproterozoic|Neoproterozoic|Age: 802 +/- 10 Ma.||||||
27299|Rook Tuff|37854|2|Defined|p10|Adelaidean|Adelaidean|Prob.Late Willouran||||||
27299|Rook Tuff|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Willouran||||||
27299|Rook Tuff|40294|6|Mentioned|p9|||||||||
27299|Rook Tuff|41363|5|Briefly described|p19|||||||||
27299|Rook Tuff|41402|6|Mentioned|p42|||||||||
27299|Rook Tuff|41403|4|Described|p61|||||||||
27299|Rook Tuff|42222|5|Briefly described|p12|||||||||
27299|Rook Tuff|42223|6|Mentioned|Fig.2 P36|||||||||
27299|Rook Tuff|42238|5|Briefly described|p72|||||||||
27299|Rook Tuff|43052|5|Briefly described|p175,Table 6.1|||of Curdimurka Subgroup. Age of 802+/-10 Ma.||||||
27299|Rook Tuff|44111|6|Mentioned|p.58 Fig. 2|||in Adelaide Geosyncline. 802 +/- 10 Ma.||||||
27299|Rook Tuff|60718|5|Briefly described|p49 Fig. 2, p50|Adelaidean|Adelaidean|Unconformably overlies Dome Sandstone. Geological Province: Adelaide Geosyncline.||Of Curdimurka Subgroup (Callanna Group).||Unconformably overlies Dome Siltstone.||15-APR-11
27299|Rook Tuff|61153|5|Briefly described|p344-345 Fig. 1|||Of the Callanna Group. Age: 802+/-10Ma (Fanning et al 1986). Geological Province: Adelaide Geosyncline. See also p352.||||||25-JAN-06
27299|Rook Tuff|61238|4|Described|p45, p48|Neoproterozoic|Neoproterozoic|Of the Callanna Group (Curdimurka Subgroup). Geological Province: Adelaide Geosyncline. Age: 802+/-10 Ma. Occurs in one isolated locality.||||||14-MAY-07
27299|Rook Tuff|61732|5|Briefly described|p4 Fig. 3|Willouran|Willouran|Of the Callanna Group.  Age: 802+/-10Ma. Geological Province: Adelaide Rift Complex/Stuart Shelf.||||||07-FEB-11
27299|Rook Tuff|62453|3|Fully described|p12 Fig. 8, 24|Cryogenian|Cryogenian|Geological Province: Adelaide Rift Complex/Stuart Shelf. Age: 802 +/- 10Ma (Fanning et al., 1986). Of the Callanna Group. Overlies Coominaree Dolomite.||||||30-AUG-18
27299|Rook Tuff|62664|5|Briefly described|p138 Fig.2, p139, p151.|Neoproterozoic|Neoproterozoic||802 +/- 10 Ma (Fanning et al. 1986)|Unit in Curdimurka Subgroup.|||Thin dacitic volcaniclastic unit.|
27299|Rook Tuff|62893|6|Mentioned|p17|||Willouran Ranges. Early Adelaidean.||||||
27299|Rook Tuff|63224|5|Briefly described|p8|Neoproterozoic|Neoproterozoic|Geological Province: Adelaide Geosyncline and Arrowie Basin.||||||07-FEB-08
27299|Rook Tuff|63562|5|Briefly described|p345|Cryogenian|Cryogenian|Adelaide Rift Complex. Mentioned as a possible, though unlikely, distal source of zircons in Grant Bluff Formation (Georgina Basin) and Cyclops Member (Amadeus Basin).|802 Ma (Fanning et al., 1986).||||Felsic.|
27299|Rook Tuff|64647|5|Briefly described|p44, p46|Willouran|Willouran|Age: 802+/-10Ma (Fanning et al. 1996).||||||
27299|Rook Tuff|64793|6|Mentioned|p283, p285|Neoproterozoic|Neoproterozoic||802 +/- 10 Ma (Fanning et al., 1986).|Curdimurka Subgroup||||
27299|Rook Tuff|64796|5|Briefly described|p183 Fig.2, p184|Cryogenian|Cryogenian||802 +/- 10 Ma (U-Pb zircon; Fanning et al., 1986)|Unit in Curdimurka Subgroup.||||
27299|Rook Tuff|64797|6|Mentioned|p153 Fig.2|Cryogenian|Cryogenian|Adelaide Rift Complex. Lithology/rank not shown on diagram.||||||
27299|Rook Tuff|64801|6|Mentioned|p111|Tonian|Tonian||802 +/- 10 Ma (Fanning et al., 1986).|Callanna Group.||||
27299|Rook Tuff|65365|5|Briefly described|p10 Fig. 4|Cryogenian|Cryogenian|Of Curdimurka Subgroup. Dated at 802 +/- 10 Ma, U-Pb (Fanning, 1986).||||||19-MAR-12
27299|Rook Tuff|65366|5|Briefly described|p23 Fig. 3, p24|Cryogenian|Cryogenian|Of Curdimurka Subgroup. Dated at 802 +/- 10 Ma, U-Pb (Fanning, 1986). Overlies the Coominaree Dolomite.||||||19-MAR-12
27299|Rook Tuff|65410|5|Briefly described|p72.|Neoproterozoic|Neoproterozoic|Age suggests that sedimentation in the Adelaide Geosyncline and Centralian Superbasin began before 800 Ma.|802 +/- 10 Ma (U-Pb; Fanning et al. 1986).|Unit in Callanna Group.||||
27299|Rook Tuff|66522|5|Briefly described|p19.|Neoproterozoic|Neoproterozoic||802 +/- 10 Ma.|Unit in Curdimurka Subgroup.||||
27299|Rook Tuff|67536|5|Briefly described|Map Legend|Cryogenian|Cryogenian||ca. 802 +/- 10 Ma||||Felsic volcanic rocks.|
27299|Rook Tuff|67979|5|Briefly described|p528|Cryogenian|Cryogenian|Age date from Willouran Ranges.|802+/-10 Ma, U-Pb zircon, Fanning et al. 1986|Curdimurka Subgroup||||
27299|Rook Tuff|69019|5|Briefly described|p37.|Neoproterozoic|Neoproterozoic||802 +/- 10 Ma (U-Pb zircon: Fanning et al. 1986).|Unit in Curdimurka Subgroup.||||
27299|Rook Tuff|69666|5|Briefly described|p33|Neoproterozoic|Neoproterozoic|Willouran Ranges.|802 +/- 10 Ma (U-Pb zircon: Fanning et al. 1986).|Curdimurka Subgroup.||||
27299|Rook Tuff|69873|5|Briefly described|p82|||Adelaide Rift Complex. Included in diagram showing Cryogenian-Ediacaran stratigraphy and correlations with Tasmanian succession.|802 +/- 10 Ma (Fanning et al., 1986).|Unit in Curdimurka Subgroup.||||21-DEC-15
27299|Rook Tuff|70819|6|Mentioned|p13|Neoproterozoic|Neoproterozoic|Clare Valley.|802 +/- 10 Ma (U-Pb).|Curdimurka Subgroup.||||
27299|Rook Tuff|72238|5|Briefly described|p42|Tonian|Tonian|Of Adelaide Geosycline.|802+\-10 Ma (Fanning et al., 1986)|||||
27299|Rook Tuff|72492|5|Briefly described|p2 Fig.1, p2|Neoproterozoic|Neoproterozoic|In Willouran Ranges. Dates from Fanning et al., 1986.|802 +/- 10 Ma|Curdimurka Subgroup||Overlies Dome Sandstone and underlies Dunns Mine Limestone.|Includes siltstone with porphyritic dacite lenses.|
27299|Rook Tuff|73188|6|Mentioned|p315|Tonian|Tonian||ca 800 Ma|||||
27299|Rook Tuff|73222|6|Mentioned|p7|Tonian|Tonian|Willouran Ranges. Torrensian.||Curdimurka Subgroup, Callanna Group, Warrina Supergroup||Underlain by Dome Sandstone. Overlain by Dunns Mine Limestone. Possibly equivalent to Wirrawilka Beds.||
27299|Rook Tuff|73262|6|Mentioned|p581, p583|Tonian|Tonian|Marks the second phase of [Rodinian] rifting. Geochron from Fanning et al. (1986).|802 +/- 10 Ma|Callanna Group, Warrina Supergroup||||
27299|Rook Tuff|74367|5|Briefly described|p7 Fig.6, p8, p12, p18-20|Tonian|Tonian|Coeval with Oodla Wirra Volcanics.|802+/-10 Ma U-Pb SHRIMP igneous zircon|Curdimurka Subgroup||||
78748|Roopena Basalt|70659|2|Defined|Throughout.|Mesoproterozoic|Mesoproterozoic|Named after Roopena Homestead. First described as the Roopena lavas (Crawford and Forbes, 1969); later the Roopena Volcanics (Blissett et al., 1993; Giles and Teale, 1979). Type locality (725175 mE, 6376650 mN, GDA 94 zone 53) and reference drillholes details given. Up to 250m thick. Gawler Craton. Described and illustrated in great detail. Graphic core logs. Derived from small amounts of partial melting of a mantle source in a back arc basin. Basalt has N-MORB to island arc chemistry and is enriched in LILE over HFSE.||Lower Gawler Range Volcanics.||Overlies Angle Dam Volcanics, Moonabie Formation, Wandearah Formation. Conformably interlayered with Fresh Well Formation. Overlain by Eucarro Rhyolite and Pandurra Formation.|Plagioclase-phyric to aphyric basaltic lavas with altered, brecciated and amygdaloidal flow tops with local minor hyaloclastite and peperite. Secondary groundmass is dominated by chlorite, clay, K-feldspar, calcite, quartz and opaques.|06-FEB-17
78748|Roopena Basalt|70816|4|Described|p1,3-4,6-p7,17-18, 19|Mesoproterozoic|Mesoproterozoic|Geological province: Spencer Domain, Gawler Craton. Roopena-Myall Creek area, Gawler Ranges. Lithological description from RC 1 drill core. Occurs most extensively in Roopena area with 13 lava flows, total thickness of up to 250m (McAvaney and Wade 2015).  Crops out ~20km south of RC1 drillhole.||Unit of lower Gawler Range Volcanics.||Conformably interlayered with Fresh Well Formation. Overlain by the Eucarro Rhyolite.|Subaerial basaltic flow with amygdaloidal, autobrecciated flow tops: plagioclase microlites, lesser lathshaped plagioclase phenocrysts in a groundmass with remnant granular to subophitic texture altered to chlorite, iddingsite, calcite.|30-MAY-19
78748|Roopena Basalt|70948|4|Described|p973,974, 975, 977, 979-983,984|Mesoproterozoic|Mesoproterozoic|Geological province: Gawler Craton. Where exposed along the SE margin of Gawler Ranges, comprises volcanoclastic lacustrine sediments interlayered with  subaerial basaltic lavas. Detailed mineralogical analysis described.||Unit of lower Gawler Range Volcanics.|||Plagioclase-rich phyric to aphyric basalt flows, composed of altered, brecciated amygdaloidal flow tops and amygdale-poor flow bases, with massive middles.|
78748|Roopena Basalt|71037|5|Briefly described|p21,  p22-23 Fig.2, p27 Fig.6, p27|Mesoproterozoic|Mesoproterozoic|Shown as occuring in the south western part of the Six Mile Hill 1:75,000 surface geology map (p22-23 Fig.2).||Gawler Range Volcanics (Lower)||Overlies Fresh Well Formation and shown as older than Spearfelt Rhyodacite.|Basalt, altered amygdale-rich or brecciated flow tops, altered and brecciated bases, local peperite and hyaloclastite.|
78748|Roopena Basalt|71129|3|Fully described|p35,47,53,59,64,68-69,75,78-84|Calymmian|Calymmian|Geological Province: Gawler Craton. Type locality: area around Roopena Homestead, 725175mE, 6376650mN, extending 1.5km E and 3.5km W (McAvaney and Wade, 2015b). Reference sections: Drillhole ROOEPNA DDH 3 (19847), 725092mE, 6377130mN, between 0-141.43m, and Drillhole ROOPENA DDH 6 (19915), 724922mE, 6376828mN, between 4.6-20m and 105.58-116.7m (McAvaney and Wade, 2015b). Flat-lying sequence of basaltic lavas; exposed and/or intersected by drilling in Roopena and Myall Creek areas. Distribution restricted to a fault-bound basin between Roopena and Wizzo Well faults (McAvaney and Wade, 2015b). Exposed as subcrop or rare weathered outcrop extending over an area ~6 km EW by 11 km NS. around the Roopena Homestead. Thickness: each flow is between 5-25m thick. Interlayered with Fresh Well Formation, and divisible into upper (comprising 11 basalt flows) and lower (comprising two basaltic flows) sections. Base of flows are typically chloritised or haematised or brecciated. Some flows contains hyaloclastite breccia. Tops of flows are amygdale-rich or auto-brecciated, typically choritised or haematised. Interleaving relationship of Roopena Basalt with Fresh Well Formation volcaniclastic lacustrine sediments indicate cyclic volcanism within periods of quiescent sedimentation; peperitic contacts indicate emplacement in wet unconsolidated sediment. Interpreted to have been deposited in a dominantly subaerial environment. Age is constrained by c. 1587+\-15 Ma age of tuffaceous unit in upper Fresh Well Formation, and c. 1591 Ma U-Pb CA-TIMS age of the overlying Spearfelt Rhyodacite. See also p93-94,114,144,184,199,202,206,225,227,230.|c. 1587 Ma|Unit of Gawler Range Volcanics.||Interlayered with Fresh Well Formation. Overlain by Spearfelt Rhyodacite. Underlain by Moonabie Formation or Wandearah Formation or Angle Dam Volcanics.|Sequence of plagioclasephyric to aphyric basalt flows with altered, brecciated and amygdaloidal flow tops, brecciated and altered bases and amygdale-poor massive middle sections, with local volcaniclastic basaltic sandstone facies.|13-NOV-19
78748|Roopena Basalt|71130|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|||Lower Gawler Range Volcanics.|||Basalt, altered amygdale-rich or brecciated flow tops, altered and brecciated bases, local peperite and hyaloclastite.|
78748|Roopena Basalt|71131|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|||Lower Gawler Range Volcanics.|||Basalt, altered amygdale-rich or brecciated flow tops, altered and brecciated bases, local peperite and hyaloclastite.|
78748|Roopena Basalt|71414|6|Mentioned|p42 Fig 1, p43|Mesoproterozoic|Mesoproterozoic|Geological province: Gawler Craton. Up to 250m thick.||Unit of Gawler Range Volcanics.||Interlayered with volcaniclastic fluvio-lacustrine Fresh Well Formation.||
78748|Roopena Basalt|71712|5|Briefly described|p411|Calymmian|Calymmian||1587 +\- 15 Ma|||Deposited contemporaneously with Gawler Range Volcanics. Possibly correlated to Corunna Conglomerate.||
78748|Roopena Basalt|72089|4|Described|p2-p5, p7-p8, p11, p15-p16, p21-p22|||Gawler Craton. ~300m of mafic volcanic rocks, previously mapped as this unit are reinterpreted as the 'Upper mafic volcanic unit' in addition to ~160m of mafic volcanics reinterpreted as an informal "mafic volcanic unit' of the Gawler Range Volcanics.||Gawler Range Volcanics, lower||Intercalated with the Fresh Well Formation and the Angle Dam Volcanics.|Dominantly basaltic lava flows including aphyric to sparsely porphyritic basalt most of which have amygdaloidal tops and some hyaloclastite.|
78748|Roopena Basalt|72090|4|Described|p12, p14, p30-p31|||Gawler Craton. Intersected in MSDP01, MSDP03 and MSDP04. See also p39-p42, p44, p95, p107.||Gawler Range Volcanics, Lower|||Olive grey, amygdaloidal, fine-grained basalt; autobrecciated flow tops; minor volcaniclastic units.|
78748|Roopena Basalt|72237|5|Briefly described|p29,32|Mesoproterozoic|Mesoproterozoic|Geological province: Gawler Craton. Of Roopena Basin.||Unit of Gawler Range Volcanics.||||
78748|Roopena Basalt|73110|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|||Lower Gawler Range Volcanics.|||Basalt; altered amygdale-rich or brecciated flow tops, altered and brecciated bases, flows ~5 to 25 m thick.|
78748|Roopena Basalt|73162|4|Described|p447-448, p450, 451,453, 455, p458-460|Calymmian|Calymmian|Roopena Basin. Correlated with mafic lavas in the Gawler Range Volcanics on basis of geochemical affinities. Minimum age constrained by overlying 1591.2+/-0.5 Ma Spearfelt Rhyodacite.||lower Gawler Range Volcanics|lower Roopena Basalt, upper Roopena Basalt|Overlies Angle Dam Dacite. Interlayered with, and overlies Fresh Well Formation. Conformably overlain by Spearfelt Rhyodacite.|Up to 13 basalt lava flow units with amygdaloidal and auto-brecciated flow-top facies, local hyaloclastic breccia.|
78748|Roopena Basalt|73234|6|Mentioned|p5|||||||||
81154|Roopena Basalt, lower|70816|4|Described|p5,17, 18|||Roopena-Myall Creek area, Gawler Ranges. See also Roopena Basalt.||Unit of lower Gawler Range Volcanics.||Interfingered with Fresh Well Formation. Contains 2 basaltic flows. Overlain by upper Fresh Well Formation. Underlain by lower Fresh Well Formation.||
81154|Roopena Basalt, lower|71129|4|Described|p69-70,73,82|Calymmian|Calymmian|Geological Province: Gawler Craton. Comprises 2 subaerial basaltic flows.||Unit of Gawler Range Volcanics.||Overlain by upper Fresh Well Formation. Underlain by lower Fresh Well Formation.|Sequence of plagioclasephyric to aphyric basalt flows with altered, brecciated and amygdaloidal flow tops, brecciated and altered bases and amygdale-poor massive middle sections, with local volcaniclastic basaltic sandstone facies.|
81154|Roopena Basalt, lower|72237|4|Described|p28,30-31|Mesoproterozoic|Mesoproterozoic|Geological province: Gawler Craton. Of Roopena Basin. Contains local hyaloclastic breccia, indicating rapid quenching of lava due to interaction with water or wet sediment in the basin.||Unit of Gawler Range Volcanics.||Overlain by upper Fresh Well Formation. Underlain by lower Fresh Well Formation.||
81154|Roopena Basalt, lower|73162|4|Described|p453, p455, p458|Mesoproterozoic|Mesoproterozoic|Roopena Basin. Thickness of 5-30 m.||Roopena Basalt||Conformably overlies Angle Dam Dacite, lower Fresh Well Formation. Underlies upper Fresh Well Formation.|Basalt with euhedral plagioclase phenocrysts; laterally variable volcanic facies with common amygdaloidal tops, in places auto-brecciated; lower base of hyaloclastite breccia in places.|
81155|Roopena Basalt, upper|70816|4|Described|p5,17-18|||Roopena-Myall Creek area, Gawler Ranges. See also Roopena Basalt.||Unit of lower Gawler Range Volcanics.||Interfingered with Fresh Well Formation. Contains 11 basaltic flows. Underlain by lower Fresh Well Formation.||
81155|Roopena Basalt, upper|71129|4|Described|p69-70,73,82|Calymmian|Calymmian|Geological Province: Gawler Craton. Comprises 11 subaerial basaltic flows.||Unit of Gawler Range Volcanics.||Underlain by upper Fresh Well Formation.|Sequence of plagioclasephyric to aphyric basalt flows with altered, brecciated and amygdaloidal flow tops, brecciated and altered bases and amygdale-poor massive middle sections, with local volcaniclastic basaltic sandstone facies.|
81155|Roopena Basalt, upper|72237|4|Described|p28,30-31|Mesoproterozoic|Mesoproterozoic|Geological province: Gawler Craton. Of Roopena Basin. Uppermost preserved unit of the Roopena Basin and contains up to 11 distinct lava flows. Characterised by thin sedimentary intervals and peperitic contacts, indicating basaltic emplacement within wet and unconsolidated sediments.||Unit of Gawler Range Volcanics.||Underlain by upper Fresh Well Formation.||
81155|Roopena Basalt, upper|73162|4|Described|p453, p455, p458, p459|Mesoproterozoic|Mesoproterozoic|Roopena Basin. Thickness of 16-235 m, extends over the whole of the basin area.||Roopena Basalt||Conformably overlies Fresh Well Formation.|Up to 11 basalt lava flow units, auto-brecciated or amygdaloidal tops; minor local basalt-sandstone peperite.|
75987|Rouge Mudstone Member|66761|2|Defined|p257 App 1, p245, 247-249, 252-253,|Early Cambrian|Early Cambrian|New Name. 3m in type section. Trilobite fossils. Age: Cambrian Series 2 Stage 4||Basal member of the Marsden Sandstone.||Conformably overlies White Point Conglomerate.|Buff coloured, calcareous mudstone. Iron stained and carbonate filled burrows.|14-MAR-12
75987|Rouge Mudstone Member|67344|5|Briefly described|p261|Early Cambrian|Early Cambrian|~ 3m thick. Contains the emuellid trilobite Balcoracania dailyi. Age defined by the parent Marsden Sandstone.||Of the Marsden Sandstone.|||Bioturbated calcareous mudstone.|
75987|Rouge Mudstone Member|73247|5|Briefly described|p204-207, p209|||Established by Gehling et al. (2011). 3 m thick. Occurs at the base of the Marsden Sandstone. Contains Balcoracania dailyi. Fossil evidence is used to correlate the unit with the Smith Bay Shale from the western succession.||Marsden Sandstone, Kangaroo Island Group.||Underlain by White Point Conglomerate. Equivalent to Smith Bay Shale and Kanmantoo Group.|Calcareous mudstone.|03-FEB-23
29936|Rowland Flat Sand|43052|5|Briefly described|Table 2.1 p26|Late Miocene|Oligocene|Barossa Basin.||||||
29936|Rowland Flat Sand|43053|5|Briefly described|Map Legend|Pliocene|Miocene|Fluviolacustrine sediments, including lignite. Geological Province: Barossa Basin.||||||
29936|Rowland Flat Sand|43258|5|Briefly described|Map Legend|Pliocene|Miocene|||||||
29936|Rowland Flat Sand|43298|5|Briefly described|Map Legend|Pliocene|Miocene|||||||
29936|Rowland Flat Sand|44133|5|Briefly described|p173|Early Pliocene|Late Oligocene|Maximum Thickness: ~110m. Geological Province: Barossa Basin. Formerly Rowland Flat Sands. ||||||
29936|Rowland Flat Sand|60953|5|Briefly described|Map Legend|Pliocene|Miocene|Fluviolacustrine sediments, including lignite. Geological Province: Barossa Basin.||||||
29936|Rowland Flat Sand|61108|5|Briefly described|map legend|Pliocene|Miocene|Fluviolacustrine sand, silt, clay and lignite. Geological Province: Barossa Basin.||||||
29936|Rowland Flat Sand|73188|6|Mentioned|p310|Miocene|Oligocene|Barossa Valley. Overlaps the Meadows Fault.||||||
28003|Roxby Downs Granite|22430|6|Mentioned|p2||Proterozoic|||||||
28003|Roxby Downs Granite|22629|5|Briefly described|p159|Calymmian|Calymmian|Age: 1590Ma. A member of Burgoyne Batholith||||||
28003|Roxby Downs Granite|22645|6|Mentioned|Fig4 P204||Proterozoic|Age of unit is 1588+/-4 Ma||||||
28003|Roxby Downs Granite|23248|6|Mentioned|p180-1|||||||||
28003|Roxby Downs Granite|23805|5|Briefly described|p4|||Pink to red-coloured, undeformed, unmetamorphosed, coarse to medium-grained, quartz-poor syenogranite with A-type affinities.  Age: 1588+/-4Ma (SHRIMP).  Geological Province: Gawler Craton.||||||
28003|Roxby Downs Granite|24168|5|Briefly described|p634|||Parent: Hiltaba granite suite.||||||
28003|Roxby Downs Granite|24197|5|Briefly described|p30, p74 Tb. 8.1|Mesoproterozoic|Mesoproterozoic|Of the Hiltaba Suite (Roxby Downs type). Age: 1592Ma. Geological Province: Gawler Craton.||||||07-FEB-11
28003|Roxby Downs Granite|24261|4|Described|p1046|Calymmian|Calymmian|Geological Province: Gawler Craton. Age: ~1588 +/- 4Ma (U-Pb zircon). Parent: Hiltaba Suite||||||
28003|Roxby Downs Granite|43052|5|Briefly described|Table 5.6|||of Hiltaba Suite. Age 1588 +/-4 Ma, U-Pb zircon.||||||
28003|Roxby Downs Granite|50605|5|Briefly described|p(ii), 1.3, 8.1, Table 1.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Gawler Craton & Curnamona Province. Of the Roxby Downs suite. Age: 1588 +/- 4Ma (U-Pb).||||||
28003|Roxby Downs Granite|60515|5|Briefly described|p120, p124 Fig.8||||c.1590 Ma.|||Hosts the Olympic Dam Breccia Complex.||
28003|Roxby Downs Granite|61522|5|Briefly described|p4|||Hosts the Olympic dam Breccia Complex which contains the Olympic Dam orebody.||||||
28003|Roxby Downs Granite|64131|6|Mentioned|p1400 |||Hosts Olympic Dam deposit.||Unit in Hiltaba Suite.||||
28003|Roxby Downs Granite|64133|6|Mentioned|p1447 Tb.1||||||Includes Olympic Dam Breccia Complex.|||
28003|Roxby Downs Granite|64319|6|Mentioned|p362|||Hosts the world-class, magmatic-hydrothermal U-Cu-Au Olympic Dam deposit.||Unit in Hiltaba Suite.||||
28003|Roxby Downs Granite|64559|5|Briefly described|p976, p977, p977 Fig. 11, p978, 980|||Age: 1588+/-4Ma. Hosts Oylmpic Dam deposit. Pink-red, coarse (<2cm), hypidiomorphic equigranular to slightly porphyritic, quartz-poor syenogranite.||||||
28003|Roxby Downs Granite|64725|5|Briefly described|pp69-70.|Mesoproterozoic|Mesoproterozoic|Forms a basement high under 300m of Neoproterozoic and Cambrian sedimentary rocks.|c.1590 Ma.|Unit in the Hiltaba Suite.|Includes Olympic Dam Breccia Complex.||Coarse-grained syenogranite with A-type affinities.|
28003|Roxby Downs Granite|65376|6|Mentioned|p147.|||||Unit in Hiltaba Suite.||||
28003|Roxby Downs Granite|65390|5|Briefly described|p10, p18, p23 Fig.3, p26 Tb. 1|Calymmian|Calymmian|Olympic Domain, Gawler Craton. Of Hiltaba Suite. Contains Olympic Dam Breccia Complex, which hosts Olympic Dam Cu-U-Au-Ag-REE deposit. Age between 1592 +/- 8 Ma and 1588 +/- 4 Ma (U-Pb) coincides with timing of mineralisation at Olympic Dam. ||||||
28003|Roxby Downs Granite|66302|6|Mentioned|p47|||Olympic Domain, Gawler Craton.||Hiltaba Suite||Intrudes the Wallaroo Group.||
28003|Roxby Downs Granite|67127|4|Described|p102 fig 3.30,|Calymmian|Calymmian|South Australia hosts within hydrothermal breccia the Olympic Dam IOCG deposit. A petrographic description is provided including constituent components of the breccias. Intruded by a variety of ultramafic, mafic and felsic dykes. Breccias are interpreted to be derived from a phreato-magmatic diatreme structure. SHRIMP age constrains the maximum age of brecciation of the Olympic dam IOCG deposit. SHRIMP age derived from Creaser and Cooper, 1993.|1588 +/- 4 Ma (SHRIMP U-Pb)|||Unconformably underlies the Corraberra Sandstone Member and the Tregolana Shale Member.|Hematite-granite breccia and hydrothermal hematite-quartz breccia.|
28003|Roxby Downs Granite|70286|6|Mentioned|p885|Mesoproterozoic|Mesoproterozoic|Johnson (1993). Eastern Gawler Craton. Hosts the Olympic Dam IOCG deposit.|1595 +/- 11 Ma.|||||
28003|Roxby Downs Granite|70328|5|Briefly described|p160,162|Mesoproterozoic|Paleoproterozoic|Geological province: Gawler Craton. Chilled margins along contacts with Olympic Dam dolerite host rock. Brecciated along the contacts with the Olympic Dam dolerite and Olympic Dam Breccia Complex.|ca. 1600 Ma|||Intruded by Olympic Dam dolerite.||
28003|Roxby Downs Granite|70502|6|Mentioned|p17-19, 23-26, 29|||Gawler Craton. U and Sm isotope compositions tabulated, discussed.|~1590 Ma.||Olympic Dam Breccia Complex.|Is intruded by Gawler Range Volcanics dykes.||
28003|Roxby Downs Granite|70511|5|Briefly described|p86, 88-89, 98|Mesoproterozoic|Mesoproterozoic|Eastern Gawler Craton. Hosts the Olympic Dam Cu-U-Au-Ag (IOCG) deposit. Part of the Burgoyne Batholith.|1594 +/- 5 Ma (U-Pb zircon; Jagodzinski, 2014).|Hiltaba Suite.||Is intruded by Gairdner Dyke Swarm and Gawler Range Volcanics. Is surrounded by (?intrudes) the Hutchison Group, Donington Suite and Wallaroo Group.||
28003|Roxby Downs Granite|70659|6|Mentioned|p48|Mesoproterozoic|Mesoproterozoic|||Hiltaba Suite.||||
28003|Roxby Downs Granite|70738|6|Mentioned|p189-190|||NE Gawler Craton. Photograph, photomicrograph.||Hiltaba Suite.||Entirely surrounds the Olympic Dam Breccia Complex.||
28003|Roxby Downs Granite|70947|5|Briefly described|p959,960,961, 962, 965-971|Mesoproterozoic|Mesoproterozoic|Geological province: Gawler Craton. Abbreviated as RDG in text. Includes the Olympic Dam Breccia Complex that hosts the Olympic Dam Cu-U-Au-Ag deposit. Mineralogy discussed.|c. 1.6 Ga|Unit of Hiltaba Suite.||Intruded by Gairdner Dyke Swarm.||
28003|Roxby Downs Granite|71236|6|Mentioned|p30-p31|||Hosts the Olympic Dam deposit.|||||Weakly altered and fractured granite to weakly brecciated granite, granite breccia with a haematite matrix.|
28003|Roxby Downs Granite|72065|4|Described|p103-106,108,110-113,115,117-118,120|Calymmian|Calymmian|Geological province: Gawler Craton. Abbreviated as RDG in text. Lava type: metaluminous, ferroan, and alkalic to alkali-calcic. Occurs near the central eastern margin of the Gawler Craton. A distinct unit within the Hiltaba Suite as it hosts the Olympic Dam Breccia Complex (and Olympic Dam Cu-U-Au-Ag deposit). Comprises typical mineralogy of the Hiltaba Suite granites. Margins of the ODBC comprise a continuum progressing from fresh to sericite-altered RDG, through mineralised hematite-rich breccias, to barren hematite-quartz-barite breccias (Ehrig et al., 2012). Contains 'HS-type' crystal clusters: fine- to medium-grained magnetite-apatite+\-titanite+\-biotite-chlorite+\-zircon. Evolution of parental magma chamber after initial crystal formation within the magma chamber and formation of GRV lavas, increasing melt water content stabilises biotite and other accessory minerals to form HS-type lavas. Intersected in drillhole RD2488 which was sampled at 5m intervals.||Unit of Hiltaba Suite.|||Dominantly porphyritic, medium- to coarse-grained syenogranite to monzogranite with minor intervals of equigranular granite and quartz and feldspar microgranophyre.|10-JAN-20
28003|Roxby Downs Granite|72459|6|Mentioned|p22|||||||||
28003|Roxby Downs Granite|72488|5|Briefly described|p2 Fig.1, p3-4, 12|||Eastern Gawler Craton. Hosts the world-class Olympic Dam Cu-U-Au-Ag deposit. ID-TIMS U-Pb zircon age by Cherry et al. (2018).|1593.87 +/- 0.21 Ma|||||
28003|Roxby Downs Granite|72949|6|Mentioned|p36-37|Calymmian|Calymmian|Olympic Domain, north. Olympic Dam / Punt Hill area.  A-type granite. Related to[?] Olympic Dam Breccia Complex.|1594 +/- 0.2 Ma|Hiltaba Suite||||
28003|Roxby Downs Granite|74361|5|Briefly described|p162, 163 Fig.1, 164, 166, 168-169, 171|||See also p173-177. Gawler Craton. After the first page, it is mostly referred to as RDG throughout the article. Textures suggest shallow emplacement. Was initially overlain unconformably by Pandurra Formation (which was subsequently eroded).|1593.87 +/- 0.21 Ma.|Hiltaba Suite|Contains the Olympic Dam Breccia Complex.|Intrudes Gawler Range Volcanics. Is overlain unconformably by Nuccaleena Dolomite.||
38350|Royston Granite|23803|5|Briefly described|p29 Fig. 2|Paleoproterozoic|Paleoproterozoic|Age: ~1849Ma. Geological Province: Gawler Craton.||||||07-NOV-08
38350|Royston Granite|24585|5|Briefly described|p32|Paleoproterozoic|Paleoproterozoic|Intrudes the Gleesons Landing Granite. Age: ~1849.5Ma.||||||07-NOV-08
38350|Royston Granite|60958|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Adamellite to syenogranite, with microline,quartz, plagioclase, biotite, hornblende, apitite and zircon. Intrudes Gleesons Landing Granite and intruded by Tournefort Metadolerite. Of the Donnington Suite. Geological Province: Gawler Craton.||||||07-NOV-08
38350|Royston Granite|61121|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Adamellite to syenogranite, with microcline, quartz, plagioclase, biotite, hornblende, apatite and metamict zircon.  Foliated to undeformed. Intrudes Gleesons Landing Granite; intruded by Tournefort Metadolerite. Geological Province: Gawler Craton.||||||07-NOV-08
38350|Royston Granite|64282|5|Briefly described|Map legend|||Intrudes the hornblende micro-adamellite section of Gleesons Landing Granite. Intruded by Tournefort Metadolerite.||||||02-JUL-08
38350|Royston Granite|64313|5|Briefly described|p452-456|Paleoproterozoic|Paleoproterozoic|Of the Donington Suite. Age: 1850+/-12Ma and 1849+/-11Ma. Adamellite + syenogranite composition which intrudes Gleesons Landing Granite.  Whole rock chemistry included.||||||09-FEB-10
38350|Royston Granite|65375|4|Described|pp12-15, pp17-19, pp45-46. |Paleoproterozoic|Paleoproterozoic|Yorke Peninsula. Thought to result from melting of the host Gleesons Landing Granite. Hornblende-biotite and elongated quartz-feldspar phenocrysts indicate a lower to medium amphibolite facies.|c.1849.5 Ma.|Unit in Donington Suite.||Intrudes Gleesons Landing Granite. Is intruded by Tournefort Metadolerite dyke.|Felsic plutons or dykes, mainly of adamellite to syenogranite composition.|
38350|Royston Granite|66302|6|Mentioned|p27|Orosirian|Orosirian|Ages from Jagodzinski et al, 2006 and Zang 2006 respectively.  |1850 +/- 12 Ma to 1849 +/- 11 Ma (SHRIMP U-Pb)|Donington Suite||||
38350|Royston Granite|68131|5|Briefly described|p3 Tb.1, p6-8, p15, p17-30|||Problems with suspected laboratory contaminants are discussed in detail. The youngest rim was dated at 1771 +/- 9 Ma (?metamorphic recrystallisation). A port-tectonic dyke was dated at 1509 +/- 9 Ma. SHRIMP ages are interpreted as magmatic crystallisation dates.|1846 +/- 4 Ma; 1843 +/- 5 Ma.|Donington Suite.||Intrudes Gleesons Landing Granite.|Typically occurs as granitic dykes. Includes granite gneiss and microgranite.|13-MAY-20
38350|Royston Granite|70721|6|Mentioned|p71|||Zircon rim growth at 1771 +/- 9 Ma is recorded by Jagodzinski et al, 2006.||Donington Suite.||||
38350|Royston Granite|73107|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Gawler Craton: Yorke Peninsula, islands of Investigator Strait and DDH Investigator 1.|1850 +/- 12 - 1849 +/- 11 Ma.|Donington Suite.||Intrudes Gleesons Landing Granite. Is intruded by Tournefort Metadolerite.|Adamellite to syenogranite, with microcline, quartz, plagioclase, biotite, hornblende, apatite and metamict zircon. Foliated to undeformed.|
38350|Royston Granite|73493|6|Mentioned|p718 Fig.5|Paleoproterozoic|Paleoproterozoic|See also Royston Head Granite p732.||||||
38350|Royston Granite|73525|5|Briefly described|p19 Fig.13|Orosirian|Orosirian|Olympic Domain.|1843+/-5 Ma, 1850+/-12 Ma|Donington Suite|||Felsic intrusive.|
24484|Saint Francis Granite|24197|6|Mentioned|p74 Tb. 8.1|Paleoproterozoic|Paleoproterozoic|Age: 1625Ma.||||||07-FEB-11
24484|Saint Francis Granite|42466|5|Briefly described|Map legend|||Reserved 1991.||||||
24484|Saint Francis Granite|42470|2|Defined|p17-23|||Described as St. Francis Granite.||||||
24484|Saint Francis Granite|43052|4|Described|Table 4.6|||Actually spelt St Francis Granite. Of Saint Peter Suite.||||||14-OCT-08
24484|Saint Francis Granite|50605|5|Briefly described|p(i), 1.3, 7.1, table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Gawler Craton & Curnamona Province. Of the Saint Peter Suite.||||||07-NOV-08
24484|Saint Francis Granite|65376|6|Mentioned|p133.|||Written as St Francis Granite. Interpreted to be associated with Nuyts Volcanics, and thus older than St Peter Suite.||||||
24484|Saint Francis Granite|66302|6|Mentioned|p24|||Appears as St Francis Granite.||||||
24484|Saint Francis Granite|73302|5|Briefly described|p35|Palaeoproterozoic|Palaeoproterozoic|||||Intrudes Nuyts Volcanics.|A distinctive leucogranite.|
34338|Saint Francis Suite|22629|6|Mentioned|fig2p147|Paleoproterozoic|Paleoproterozoic|Spelt "St" in the text.||||||07-NOV-08
34338|Saint Francis Suite|60953|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Age: 1631-1627Ma. Granitoids.||||||07-NOV-08
34338|Saint Francis Suite|61108|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|Spelt St on map legend. Leucogranite and granite, often porphyritic.||||||07-NOV-08
34338|Saint Francis Suite|67536|6|Mentioned|Map Legend|||Gawler Craton. St Francis Suite in text.|||||Leucogranite and leucoporphyry.|
34338|Saint Francis Suite|73302|5|Briefly described|p34|Palaeoproterozoic|Palaeoproterozoic|Gawler Craton. Mapped on p34 as a single unit with St Peter Suite.||||Coeval with St Peter Suite and Nuyts Volcanics.||
72574|Saltbush Group|62592|5|Briefly described|p15. |||Olary Domain, Curnamona Province. Sedimentation followed igneous activity of the Lady Louise Suite.|<1685 Ma.|||||
72574|Saltbush Group|62993|5|Briefly described|p2, 4, 9,12-15,18,21,35, 37-409|Paleoproterozoic|Paleoproterozoic|Olary Domain. Misspelt as Saltbush Subgroup on p3, p20, p21.|||Includes Raven Hill Subgroup, Walparuta Formation, Larry Macs Subgroup|Equivalent to the Broken Hill Group? Or just the Purnamoota Subgroup?||19-DEC-21
72574|Saltbush Group|63866|5|Briefly described|p40||||||Includes the Plumbago Formation and the Bimba Formation.|Unconformably overlies the Ethiudna Subgroup. Equivalent to the Broken Hill and Sundown Groups.||
72574|Saltbush Group|64741|5|Briefly described|p301 Fig. 4|Paleoproterozoic|Paleoproterozoic|Of Willyama Supergroup. Includes Larry Macs and Raven Hill Subgroups. Geological province: Olary Domain, Curnamona Province.||||||29-MAR-12
72574|Saltbush Group|64944|5|Briefly described|p27, p28 Fig. 1, p29 Tb. 1|Paleoproterozoic|Paleoproterozoic|Of Willyama Supergroup. Equivalent to the combined Broken Hill and Sundown Groups in the Broken Hill Domain. Geological province: Olary Domain.||||||07-FEB-11
72574|Saltbush Group|66302|5|Briefly described|p36 Fig.9, p37, p38, p39|Statherian|Statherian|Olary Domain, Curnamona Province. |ca 1695-1670 Ma|Willyama Supergroup|Includes the Larry Macs Subgroup, Raven Hill Subgroup and the Walparuta Formation.|Unconformably overlies the Ethiudna Subgroup. Equivalent to the Broken Hill and Sundown Groups.||
72574|Saltbush Group|67323|5|Briefly described|Eastern Australia Time-Space Plot; p33|||Olary Domain, Curnamona Province. Deposited during intra-continental extension.|~1720-1690 Ma.||Raven Hill Subgroup; Walparuta, Plumbago, Bimba Formations; Lady Louise Suite.|||
72574|Saltbush Group|67653|6|Mentioned|p5,11|||Geological province: Curnamona Province. ||||||
72574|Saltbush Group|68126|5|Briefly described|p26, p30|||Olary Domain, Curnamona Province.|||Bimba, Plumbago Formations.|Equivalent to Broken Hill and Sundown Groups.||
72574|Saltbush Group|70339|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic||1693+/-3 Ma.|Willyama Supergroup.|||Psammopelite, schistose; psammite layers, locally graded; minor tourmalinite; Mn-coticules and iron-formation near base.|02-FEB-16
72574|Saltbush Group|70405|5|Briefly described|p15, p25, p43 Table 3, p96|Paleoproterozoic|Paleoproterozoic||1665 Ma-1680 Ma||Includes Larry Macs Subgroup, Raven Hill Subgroup, Walparuta Formation||Primarily composed of volcaniclastic sediments and metasediments with interfingering or carbonates. Base metal concentrations (Sedex) occur throughout this group.|
72574|Saltbush Group|70657|4|Described|p5, p6 Fig.1, p11 Fig.5, p12, p13 Fig.6|Statherian|Statherian|See also p14-17, p19-21, p24, p33-34, p37, p40-43, p57-58, p63-66, p77. Curnamona Province, Olary Domain. Formerly Saltbush Subgroup (Conor, 2000); elevated to Group rank in this study. Includes the Bimba Formation on the basis of recent geochronology. Shown as upper Saltbush in Figs.1, 5. Fig.6 suggests that the Raven Hill Subgroup in Olary Domain is part of the Broken Hill Group. Lack of outcrop has hindered geological understanding. Upper parts have restricted continuity, particularly in the north. Significant but low-grade Zn-(Pb) mineralisation; local Mn-enrichment.|<1705 Ma, >1655 Ma|Willyama Supergroup|Includes Larry Macs and Raven Hill Subgroups, Walparuta Formation.|Underlies Strathearn Group. Overlies Curnamona Group, and Portia Formation (in Mulyungarie Domain). Equivalent to the combined Broken Hill and Sundown Groups.|Dominantly siliciclastic metasediments, mainly psammopelite with thick pelitic intervals and thin psammite layers.|
72574|Saltbush Group|70658|5|Briefly described|p7, 10, 15, 23, 42, 47|Paleoproterozoic|Paleoproterozoic|Olary Domain, Curnamona Province.||Willyama Supergroup.|Larry Macs, Raven Hill Subgroups; Walparuta Formation.|Is overlain by Strathearn Group.||
72574|Saltbush Group|73429|5|Briefly described|p106 Fig.2, p107, p110, p111 Fig.6|Statherian|Statherian|Curnamona Province, Olary Domain. Overlies regional unconformity. Characterised as a low magnetic response unit.||Willyama Supergroup, upper|Larry Macs Subgroup, Raven Hill Subgroup, Walparuta Formation|Unconformably overlies Curnamona Group, underlies Strathearn Group||
80435|Samphire Granite|71536|5|Briefly described|p10, p22, p24-p25, p27-p28|||?p2? p3? Geochem data p24-25. Compared with Charleston Granite. Uranium values compared with those of zircons in the palaeochannel sand of the Samphire U deposit.[Although not clearly stated, it appears, from p22 that samples1948989, 1948990, 1948992, 1948993, 1948994 and 1948995, from drillholes MRC009, MRC007A and MRC005 are all considered to be Samphire Granite, Hiltaba Suite].|1584+/-4,  1586+/-6 Ma U/Pb zircon SHRIMP||||Coarse-grained granite.|18-JAN-22
23955|Sandison Subgroup|7931|5|Briefly described|p99 Fig. 2|Ediacaran|Ediacaran|Incudes Nuccaleena and Brachina Formations, and ABC Range Quartzite.||||||07-FEB-11
23955|Sandison Subgroup|23211|6|Mentioned|p43,44,46 Fig.2|||Of Wilpena Group.||||||13-FEB-08
23955|Sandison Subgroup|23287|6|Mentioned|Fig.3|||Of Wilpena Group. Age: Lower Ediacarian.||||||13-FEB-08
23955|Sandison Subgroup|24195|5|Briefly described|p45 Fig.3|||Max Thickness: ~1000m at Hallett Cove. Geological Province: Adelaide Geosyncline||||||
23955|Sandison Subgroup|24586|5|Briefly described|p50 Fig. 1, p51 Fig. 1|Adelaidean|Adelaidean|Of the Wilpena Group (Heysen Supergroup). Includes ABC Range Quartzite, Brachina and Nuccaleena Formations and Seacliff Sandstone. Geological Province: Adelaide Geosyncline.||||||05-JUL-06
23955|Sandison Subgroup|42600|2|Defined|p2-13|||Reserved 1988. Defined in Hallett Cove area. Does not include younger Bunyeroo and Wonoka Formations.|||Includes Nuccalena Formation, Seacliff Sandstone, Brachina Formation, ABC Range Quartzite.|||23-JAN-19
23955|Sandison Subgroup|42763|4|Described|p20|||see also Fig.2 p21, Fig.3 p23||||||11-NOV-22
23955|Sandison Subgroup|42882|5|Briefly described|Table 1 p3|||Of Wilpena Group.||||||11-NOV-22
23955|Sandison Subgroup|43622|6|Mentioned|p38|Neoproterozoic||||||||
23955|Sandison Subgroup|43845|5|Briefly described|Fig2 p42, 46||Neoproterozoic|In Wilpena Group.||||||12-JUL-16
23955|Sandison Subgroup|60718|5|Briefly described|p49 Fig. 2|Adelaidean|Adelaidean|Geological Province: Adelaide Geosyncline.||Of Wilpena Group.||Includes ABC Range Quartzite, Brachina and Nuccaleena Formations.||15-APR-11
23955|Sandison Subgroup|60889|6|Mentioned|p250 Fig.7|||||||||
23955|Sandison Subgroup|60959|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Of the Wilpena Group.||||||
23955|Sandison Subgroup|61732|5|Briefly described|p28 Fig. 13|Marinoan|Marinoan|Includes ABC Quartzite, Brachina and Nuccaleena Formations, and Seacliff Sandstone. Geological Province: Adelaide Rift Complex||||||07-FEB-11
23955|Sandison Subgroup|62592|5|Briefly described|p50 Table 5.1.|Ediacaran|Ediacaran|Adelaide Geosyncline.||Unit in Wilpena Group.|Includes Nuccaleena and Brachina Formations and ABC Range Quartzite.|Is disconformably overlain by Bunyeroo Formation.||
23955|Sandison Subgroup|64282|5|Briefly described|Map legend|Neoproterozoic III|Neoproterozoic III|Represented on this map by undifferentiated rocks of grey andalusite schist and metasiltstone. Geological Province: Adelaide Geosyncline.||||||01-JUL-08
23955|Sandison Subgroup|64455|5|Briefly described|p138 Fig. 1|Ediacaran|Cryogenian|Of Wilpena Group. Includes Nuccaleena and Brachina Formations and ABC Range Quartzite.||||||29-JAN-09
23955|Sandison Subgroup|65892|5|Briefly described|p32.|Ediacaran|Ediacaran|Adelaide Geosyncline.|||Includes Seacliff Sandstone, Brachina Formation, ABC Range Quartzite.|||
23955|Sandison Subgroup|65925|5|Briefly described|Appendix 2.||||||||Sandstone; mudstone. Marine shelf and slope deposits, some shore face.|
23955|Sandison Subgroup|67870|5|Briefly described|p9|Ediacaran|Ediacaran|Adelaide Rift System.||Wilpena Group.|Nuccaleena, Brachina, ABC Range Formations.|||
23955|Sandison Subgroup|69019|5|Briefly described|p54.|Neoproterozoic|Neoproterozoic|Of Dyson (1992) and Miller and Schuring (1993).||Unit in Wilpena Group.|Includes Seacliff Sandstone, Nuccaleena Formation, Ulupa Siltstone, Brachina Formation, ABC Range Quartzite.|||
23955|Sandison Subgroup|70334|5|Briefly described|p20,30,56|||Geological province: Gawler Craton. Of Adelaide Geosyncline and Stuart Shelf. ||Unit of Wilpena Group.|Includes ABC Range Quartzite, Brachina Formation Tent Hill Formation, Nuccaleena Formation and Seacliff Sandstone.|||
23955|Sandison Subgroup|70384|5|Briefly described|Map legend.|Ediacaran|Neoproterozoic|Adelaide Geosyncline.||Wilpena Group.|Nuccaleena Formation, Ulupa Siltstone.|Unconformably overlies Yerelina Subgroup (Umberatana Group).||23-JAN-19
23955|Sandison Subgroup|70406|5|Briefly described|p119, p121 Fig 5, p124, 127|Neoproterozoic|Neoproterozoic|Stuart Shelf.  Thickness affected by syn-depositional tectonics in Adelaide Geosyncline.||Of Wilpena Group.|Includes Seacliff Sandstone, Nuccaleena Formation, Brachina Formation, ABC Range Quartzite, Tent Hill Formation, Simmens Quartzite.|||29-APR-16
23955|Sandison Subgroup|70407|5|Briefly described|p102 Fig 1, p103 Fig 2, p106, p112|Neoproterozoic|Neoproterozoic|Age: Ediacaran.||Of Wilpena Group.||Unconformably overlain by Aruhna Subgroup.||
23955|Sandison Subgroup|71129|5|Briefly described|p128|Ediacaran|Ediacaran|Of Stuart Shelf.||Of the Wilpena Group.|Includes ABC Range Quartzite and Brachina Formation.|||13-NOV-19
23955|Sandison Subgroup|73188|5|Briefly described|p315-316, p352|Ediacaran|Ediacaran|Mount Lofty Ranges.||Wilpena Group|ABC Range Quartzite, Brachina Formation, Nuccaleena Formation, Seacliff Sandstone||Includes siltstone and quartzite.|
23955|Sandison Subgroup|73222|6|Mentioned|p6, p11, p16, p24|Ediacaran|Ediacaran|Adelaide Rift Complex.||Wilpena Group, Heysen Supergroup|ABC Quartzite, Brachina Formation|||
23955|Sandison Subgroup|73236|5|Briefly described|p36, p38, p47|Ediacaran|Ediacaran|Marine sedimentary rocks. Transgressive-regressive sequence.|c. 635-600 Ma|Wilpena Group, Heysen Supergroup|ABC Range Quartzite, Brachina Formation, Nuccaleena Formation, Seacliff Sandstone|[Unconformably] underlain by Reynella Siltstone Member (Elatina Formation, Yerelina Subgroup, Umberatana Group).||
23955|Sandison Subgroup|74367|5|Briefly described|p7 Fig.6, p8, p22|Ediacaran|Ediacaran|Misspelt Sandision p8.|||Nuccaleena Formation, Brachina Formation, ABC Range Quartzite|||
38068|Sea Lion Supersequence|23792|5|Briefly described|p56, Fig.D4|Kimmeridgian|Callovian|Fluvial and lacustrine clastic sediments. Equivalent to Polda Formation. Overlain by Minke supersequence. Geological Province: Bight Basin. Off shore.||||||04-MAY-05
38068|Sea Lion Supersequence|24336|5|Briefly described|p99 Fig.3|||Correlated to the Polda Formation Equivalent.||||||
38068|Sea Lion Supersequence|61544|6|Mentioned|p367 Fig.3. |Kimmeridgian|Callovian|Ceduna Sub-basin. Syn-rift mechanical extension. ||||Is overlain by Minke Supersequence.||
38068|Sea Lion Supersequence|66578|6|Mentioned|p1007 Fig.3.|Late Jurassic|Jurassic|Ceduna Sub-Basin, Bight Basin.||||Is overlain by Minke Supersequence.||
38068|Sea Lion Supersequence|69297|5|Briefly described|p14 fig 2.4, p23, p25 fig 2.9|Kimmeridgian|Oxfordian|Eyre, Ceduna and Duntroon Sub-basins. Shale facies within this sequence have the best potential to be seal rocks in the Eyre Sub-basin. Good faulting seal capacity for hydrocarbons. Contains potential source rocks within lacustrine shales and coaly deposits. See also p26 fig 2.11, p27, p28, p37, p42, p45 fig 2.17, p58, p60, p61.||||Overlain by the Minke Supersequence.|Sandstone, siltstone and claystone.|
38068|Sea Lion Supersequence|70067|5|Briefly described|Ceduna: Fig.2. Regional: Fig.2|Kimmeridgian|Oxfordian|Bight Basin. The lithologies are unknown, not having been penetrated by wells.||||Is overlain by Minke Supersequence.||
25748|Seacliff Sandstone|22746|6|Mentioned|p528|Neoproterozoic III|Neoproterozoic III|||||||
25748|Seacliff Sandstone|22901|6|Mentioned|78|||Geol province Adelaide Rift Complex||||||
25748|Seacliff Sandstone|22921|6|Mentioned|37|||||||||
25748|Seacliff Sandstone|23211|6|Mentioned|p44-46|||||||||
25748|Seacliff Sandstone|23287|6|Mentioned|Fig.2-4|||Age: Lower Ediacaran. Adelaide Geosyncline.||||||05-APR-13
25748|Seacliff Sandstone|23557|5|Briefly described|p95 Fig.1|Neoproterozoic III|Neoproterozoic III|Geological Province: Adelaide Rift Complex.||||||
25748|Seacliff Sandstone|23719|4|Described|p26|||See also page 25 table 7. Of Wilpena Group. O'lain by Brachina Formation. U'lain by Umberatana Group. Geological Province: Gawler Craton. Max. thickness >120 m.||||||23-JUN-09
25748|Seacliff Sandstone|24586|5|Briefly described|p51 Fig. 1|Adelaidean|Adelaidean|Of the Sandison Subgroup (Wilpena Group, Heysen Supergroup). Geological Province: Adelaide Geosyncline.||||||
25748|Seacliff Sandstone|32724|6|Mentioned|Fig.1|||Marinoan. Correlation||||||
25748|Seacliff Sandstone|33422|6|Mentioned|Map legend|Precambrian|Precambrian|||||||
25748|Seacliff Sandstone|34536|6|Mentioned|Map legend|Adelaidean|Adelaidean|EquivalentMarinoan||||||
25748|Seacliff Sandstone|35255|5|Briefly described|p10|||See also Fig.3.||||||
25748|Seacliff Sandstone|35678|6|Mentioned|Fig.2|||Geological cross-sections, northern Yorke Peninsula.||||||
25748|Seacliff Sandstone|38110|1|Redefined|p2|Adelaidean|Adelaidean|||||||
25748|Seacliff Sandstone|38157|6|Mentioned|Table V|||||||||
25748|Seacliff Sandstone|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Marinoan||||||
25748|Seacliff Sandstone|39351|6|Mentioned|Map legend|Adelaidean|Adelaidean|Marinoan||||||
25748|Seacliff Sandstone|39352|6|Mentioned|Map legend|Adelaidean|Adelaidean|Marinoan||||||
25748|Seacliff Sandstone|40456|4|Described|p28|||Also mention Fig.2.||||||
25748|Seacliff Sandstone|40852|6|Mentioned|Fig.3.2|||||||||
25748|Seacliff Sandstone|41005|6|Mentioned|Fig.2|||||||||
25748|Seacliff Sandstone|41405|6|Mentioned|p194|||||||||
25748|Seacliff Sandstone|41429|3|Fully described|p214|||||||||
25748|Seacliff Sandstone|42098|5|Briefly described|p54|||||||||
25748|Seacliff Sandstone|42100|6|Mentioned|p70|||||||||
25748|Seacliff Sandstone|42222|6|Mentioned|Table 1 P4|||||||||
25748|Seacliff Sandstone|42235|5|Briefly described|p140|||||||||
25748|Seacliff Sandstone|42239|6|Mentioned|p160|||||||||
25748|Seacliff Sandstone|42243|6|Mentioned|p211|||||||||
25748|Seacliff Sandstone|42465|5|Briefly described|Map Legend|||||||||
25748|Seacliff Sandstone|42469|4|Described|p24|||||||||
25748|Seacliff Sandstone|42542|6|Mentioned|p13|||||||||
25748|Seacliff Sandstone|42600|4|Described|p7|||||||||
25748|Seacliff Sandstone|42720|5|Briefly described|map legend|Marinoan||||||||
25748|Seacliff Sandstone|42763|6|Mentioned|p20|||||||||
25748|Seacliff Sandstone|42813|5|Briefly described|p21|||of Wilpena Group||||||
25748|Seacliff Sandstone|43052|5|Briefly described|Table 6.1,p192|||of Wilpena Group||||||
25748|Seacliff Sandstone|43622|6|Mentioned|p38|Neoproterozoic||Sandison Subgroup, Wilpena Group.||||||
25748|Seacliff Sandstone|43845|5|Briefly described|Fig3 p43, 46||Neoproterozoic|In Umberatana Group||||||12-JUL-16
25748|Seacliff Sandstone|44133|5|Briefly described|p68, 149|Neoproterozoic|Neoproterozoic|||||||
25748|Seacliff Sandstone|61732|5|Briefly described|p4 Fig. 3, p28 Fig. 13|Marinoan|Marinoan|Of the Sandison Subgroup (Wilpena Group). Geological Province: Adelaide Rift Complex/Stuart Shelf. See also p150.||||||07-FEB-11
25748|Seacliff Sandstone|62085|6|Mentioned|p22|Ediacaran|Ediacaran|||||Correlative of Nuccaleena Formation.|Sandstone, lesser dolomite.|
25748|Seacliff Sandstone|63458|6|Mentioned|p897 Fig.19. |Ediacaran|Ediacaran|||Unit in Wilpena Group.||||
25748|Seacliff Sandstone|65365|5|Briefly described|p10 Fig. 4|Ediacaran|Ediacaran|Adelaide Rift Complex / Stuart Shelf||||||
25748|Seacliff Sandstone|65366|5|Briefly described|p23 Fig. 3|Ediacaran|Ediacaran|Adelaide Rift Complex / Stuart Shelf||||||
25748|Seacliff Sandstone|65892|5|Briefly described|p32, p34. |Ediacaran|Ediacaran|Adelaide Geosyncline. Estuarine deposits.||Basal Sandison Subgroup.||Overlies Elatina Formation.||
25748|Seacliff Sandstone|66464|6|Mentioned|p173|||Mentioned as being intertongued with Nuccaleena Formation dolostone.||||||
25748|Seacliff Sandstone|66569|5|Briefly described|p860, p861 fig.2,|Ediacaran|Ediacaran|Of Wilpena Group; Up to 340 m thick; underlies/intertongues with Nuccaleena Formation and Brachina Formation; unconformably overlies Elatina Formation/Yerelina Subgroup;||||||
25748|Seacliff Sandstone|67030|6|Mentioned|p409 Fig. 2|Ediacaran|Ediacaran|||||Overlies the Elatina Formation, underlies the Moolooloo Siltstone Member, Brachina Formation. Equivalent to the Nuccaleena Formation.||26-APR-12
25748|Seacliff Sandstone|68241|6|Mentioned|p20 Fig.1|||||||||
25748|Seacliff Sandstone|68269|6|Mentioned|p674|||Adelaide Geosyncline.||Wilpena Group||Unconformably underlain by Elatina Formation (Yerelina Subgroup). Overlain by Nuccaleena Formation.|Includes sandstone and a basal conglomerate.|
25748|Seacliff Sandstone|69019|5|Briefly described|p54-55.|Neoproterozoic|Neoproterozoic|Thomson (1966), Forbes (1982), Dyson (1992). Typically 5-15 m thick.||Unit in Sandison Subgroup.||Unconformably overlies Yerelina Subgroup. Intertongues with and underlies Nuccaleena Formation.|Pale to medium grey quartzite and sandstone, medium-grained and variably cross-bedded; lesser reddish siltstone with local thin dolomitic beds.|
25748|Seacliff Sandstone|70082|5|Briefly described|p2-4,7,15-16|Ediacaran|Ediacaran|Kulpara-Adelaide region. Also shown as Seacliff Sandstone Member on Fig 2 p2. Basal Seacliff Sandstone paleochannel incision records a local relative fall of sea level (Dyson and von der Borch, 1994);trough cross bedding indicate fluvial incision and fill (Dyson and von der Borch, 1994), creating sand-wedge paleosols during a time of relative sea level fall during frigid conditions. Also does not contain dropstones or evidence of sea ice or ice bergs (Dyson, 1983, 2002; Dyson and von der Borch, 1994).||Unit of Brachina Formation.||Underlain disconformably (channel incision to the south) by Nuccaleena Formation and Reynella Siltstone Member.||
25748|Seacliff Sandstone|70333|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic||||||Quartzite; sandstone; siltstone.|
25748|Seacliff Sandstone|70334|4|Described|p2,20,31-32,65,77,79|Ediacaran|Ediacaran|Geological province: Gawler Craton. Of Adelaide Geosyncline and Stuart Shelf. Previously suggested depositional environments include shallow water deltaic (Thomson et al., 1976), shallow shelf to proximal slope marine, with sands deposited by turbidity currents (Dyson, 1986) and an influx of sand during deposition of the Nuccaleena Formation (Preiss, 1987). Extendes along the western paleo-shoreline of the Adelaide geosyncline, with detritus derived from Gawler Craton.||Unit of Sandison Subgroup.||Overlain by Brachina Formation. Underlain by Nuccaleena Formation or Elatina Formation. Intertongued with Nuccaleena Formation.|Red-brown to purple-grey fine-grained sandstone and lithic sandstone interbedded with brown and grey siltstone.|
25748|Seacliff Sandstone|70406|5|Briefly described|p125, p121 Fig 5|||||Of Sandison Subgroup.||Shown as interfingering with Nuccaleena Formation.||
25748|Seacliff Sandstone|70407|6|Mentioned|p113|||Incised valleys associated with this unit.||||||
25748|Seacliff Sandstone|72450|5|Briefly described|Brochure, Brochure map|||Present at Hallett Cove and in road cuttings at Pedler Creek bridge. Deformed by the Delamerian Orogeny. Striated by Permian glaciers.||Base of the Wilpena Group|||Pale grey and red sandstone, quartzite and red siltstone.|
25748|Seacliff Sandstone|72456|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Marree 1:250k map sheet. |||||Quartzite, sandstone and siltstone.|
25748|Seacliff Sandstone|73110|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic||||||Quartzite; sandstone; siltstone.|
25748|Seacliff Sandstone|73188|5|Briefly described|p316, p331|Ediacaran|Ediacaran|Mount Lofty Ranges.||Sandison Subgroup, Wilpena Group|||Massive sandstone.|
25748|Seacliff Sandstone|73236|4|Described|p36-39, p41, p44-45, p47|Ediacaran|Ediacaran|Marine shelf sedimentary rocks. Rapidly deposited under post-glacial transgressive conditions, and contains dewatering structures. Responded to the compressive stresses of the Delamerian Orogeny by forming open, concentric folds and minor brittle faults. Base at Hallett Cove is a major sequence boundary, which correlates with the base of the Wilpena Group elsewhere.||Sandison Subgroup, Wilpena Group, Heysen Supergroup||[Unconformably] underlain by Reynella Siltstone Member (Elatina Formation, Yerelina Subgroup, Umberatana Group). Conformably overlain by and interfingers with Nuccaleena Formation.|Dark red-brown siltstone and shale; pale red, medium-grained blocky sandstone; pale brown, medium-grained, massive quartzite.|
27563|Seaford Formation|22525|6|Mentioned|p36,37,38||Pleistocene|sometimes combined with overlying Ochre Cove Formation as the Robinson Point Formation (old usage)||||||
27563|Seaford Formation|22941|6|Mentioned|p290|||||||||
27563|Seaford Formation|23489|1|Redefined|p45|Pleistocene|Pleistocene|Type section in article. Overlying unit Ochre Cove Formation. Lith: Medium to coarse-grained yellow, white and red mottled, partly clayey sandstone. Noarlunga Embayment. Max. thickness: 20 m.||||||
27563|Seaford Formation|24465|5|Briefly described|p351 Fig.1|Quaternary|Quaternary|||||||
27563|Seaford Formation|30757|6|Mentioned|p4|||||||||
27563|Seaford Formation|35097|6|Mentioned|Fig.4|||||||||
27563|Seaford Formation|36127|6|Mentioned|p11|||See also p7.||||||11-NOV-22
27563|Seaford Formation|38290|6|Mentioned|p55|||||||||
27563|Seaford Formation|39351|6|Mentioned|Map legend|Quaternary|Quaternary|||||||
27563|Seaford Formation|39522|6|Mentioned|p85|||||||||
27563|Seaford Formation|40442|6|Mentioned|Fig.20|||||||||
27563|Seaford Formation|41495|4|Described|p44|||||||||
27563|Seaford Formation|41513|6|Mentioned|p44|||||||||
27563|Seaford Formation|41551|6|Mentioned|p463|||||||||
27563|Seaford Formation|43682|5|Briefly described|p290|||||||||
27563|Seaford Formation|44198|2|Defined|p25|Pliocene|Pliocene|||||||
27563|Seaford Formation|44199|2|Defined|p594, 595, 597|Quaternary|Neogene|late Tertiary - Quaternary.||||||
27563|Seaford Formation|44200|6|Mentioned|p.352, 355|||||||||
27563|Seaford Formation|65901|5|Briefly described|p176, p176 Tab.1|Pleistocene|Pleistocene|Included in Hindmarsh Clay by Firman (1967). Earliest Pleistocene age.||||Base interfingers with Burnham Limestone.|Green/grey clayey sand with weak orange mottles.|08-MAR-12
27563|Seaford Formation|70660|5|Briefly described|p10, p32|Pleistocene|Pleistocene|||||||
27563|Seaford Formation|73188|5|Briefly described|p319-320, p333, p346, p351, p357-359|Pleistocene|Pliocene|St Vincent Basin and ?Mount Lofty Ranges. Fluvial. Exposed in coastal cliffs of the Noarlunga Embayment; possibly extends landward on the Mount Osmond Block as far as Belair. Includes upper Cenozoic sandstones mapped by Fairburn et al. (2010) as ""Pirramimma Sandstone"".",,||||Disconformably overlain by Ochre Cove Formation. Possibly equivalent to Pirramimma Sandstone.|Poorly bedded, yellow-buff to pale grey, fine to medium-grained, weakly indurated sand.|11-NOV-22
24491|Second Plain Creek Member|40831|2|Defined|p2|Cambrian|Cambrian|Prob. Cambrian||||||
24491|Second Plain Creek Member|42226|5|Briefly described|p231|||||||||
24491|Second Plain Creek Member|42233|6|Mentioned|p252|||See also Fig.2||||||
24491|Second Plain Creek Member|60418|5|Briefly described|p135|Early Cambrian|Early Cambrian|Of the Wilkawillina Limestone. Overlain by Mernmerna Formation.||||||
24491|Second Plain Creek Member|62784|6|Mentioned|p9|Cambrian|Cambrian|Unit in Wilkawillina Limestone, Hawker Group. Arrowie Basin.||||||20-MAR-12
24491|Second Plain Creek Member|63569|6|Mentioned|p118|Early Cambrian|Early Cambrian|||Unit in Wilkawillina Limestone.||||
24491|Second Plain Creek Member|70833|5|Briefly described|p176,178,186-187,190,193,199-201,203|Series 2|Terreneuvian|Of Arrowie Basin. Key sections: WILK (Bunkers Graben). Only crops out in the Bunkers Graben. Deposited on a starved carbonate platform during rapid transgression. Transitional between undelying relatively shallow Winnitinny Creek Member and overlying deeper outer shelf Mernmerna Formation.||Unit of Wilkawillina Limestone.||Uppermost unit of Wilkawillina Limestone.||
24491|Second Plain Creek Member|71102|6|Mentioned|p267|Series 2|Series 2|Of Arrowie Basin.||||||
35822|Sedan granite|23317|6|Mentioned|378|||||||||
33996|Semaphore Sand Member|22525|6|Mentioned|p37.41||Holocene|||||||
33996|Semaphore Sand Member|23489|5|Briefly described|p43 Table 1|Holocene|Holocene|||||||
33996|Semaphore Sand Member|60953|5|Briefly described|Map Legend|Holocene|Holocene|White calcareous and siliceous coastal dune sand.||||||
33996|Semaphore Sand Member|60958|5|Briefly described|Map Legend|Holocene|Holocene|Of the Saint Kilda Formation.  Unconsolidated, white bioclastic quartz-carbonate sand of modern beaches and transgressive dune fields.||||||
33996|Semaphore Sand Member|61070|5|Briefly described|Map Legend|Holocene|Holocene|Foredune and dune sand. White to cream quartz and shelly sand. Includes calcareous sand reworked from the Bridgewater Formation and modern beach facies. Of the Saint Kilda Formation.||||||12-JAN-10
33996|Semaphore Sand Member|61108|5|Briefly described|map legend|Holocene|Holocene|White calcareous and siliceous coastal dune sand.||||||
33996|Semaphore Sand Member|61121|5|Briefly described|Map legend|Holocene|Holocene|Of the Saint Kilda Formation. Unconsolidated, white bioclastic quartz-carbonate sand of modern beaches and transgressive dune fields.||||||
33996|Semaphore Sand Member|64282|5|Briefly described|Map legend|Holocene|Holocene|Of the Saint Kilda Formation. Unconsolidated white, bioclastic quartz carbonate sand of modern beaches and transgressive dune fields.||||||
33996|Semaphore Sand Member|65375|5|Briefly described|p42.|Holocene|Holocene|||Unit in Saint Kilda Formation.|||Modern beach and dune sand deposit.|
33996|Semaphore Sand Member|67117|5|Briefly described|Map legend.|Holocene|Holocene||||||Unconsolidated white bioclastic quartz-carbonate sand of modern beaches and transgressive dune fields.|
33996|Semaphore Sand Member|68131|6|Mentioned|p7, p12, p17, p31, p42, p66, p71|Holocene|Holocene|Yorke Peninsula. Appears as Semaphore Sand on p42.||||||
33996|Semaphore Sand Member|69048|5|Briefly described|p2|Cenozoic|Cenozoic|Southern Eyre Peninsula.||Saint Kilda Formation.||||
33996|Semaphore Sand Member|69372|6|Mentioned|p28 Fig.6, p34 fig. 12|Holocene|Holocene|||||||
33996|Semaphore Sand Member|70333|5|Briefly described|Map legend.|Holocene|Holocene||||||Unconsolidated white bioclastic quartz-carbonate sand of modern beaches and transgressive dune fields.|
33996|Semaphore Sand Member|70334|6|Mentioned|p72|||Modern beach sand along the present shoreline and stranded beach ridges within the present supratidal zone.||||||
33996|Semaphore Sand Member|70337|5|Briefly described|Map legend.|Holocene|Holocene||||||Unconsolidated white bioclastic quartz-carbonate sand of modern beaches and transgressive dune fields.|
33996|Semaphore Sand Member|70382|5|Briefly described|p29 Fig 3|Holocene|Holocene|Yorke Peninsula region.|||||Unconsolidated sand|
33996|Semaphore Sand Member|70660|5|Briefly described|p10|Holocene|Holocene|||||||
33996|Semaphore Sand Member|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sand, eolian, beach sediments, coastal sedient|
33996|Semaphore Sand Member|72450|6|Mentioned|Brochure, Brochure map|Holocene|Holocene|Largest deposits occur south of Seaford near the mouth of Pedler Creek and in Aldinga Scrub Reserve at Silver Sands.|||||Beach sand, back-beach dune sand and inland sand drift.|
33996|Semaphore Sand Member|73103|5|Briefly described|Map legend.|Holocene|Holocene||||||Unconsolidated white bioclastic quartz-carbonate sand of modern beaches and transgressive dune fields.|
33996|Semaphore Sand Member|73107|5|Briefly described|Map legend.|Holocene|Holocene||||||Unconsolidated, white bioclastic quartz-carbonate sand of modern beaches and transgressive dune fields.|
33996|Semaphore Sand Member|73110|5|Briefly described|Map legend.|Holocene|Holocene||||||Unconsolidated white bioclastic quartz-carbonate sand of modern beaches and transgressive dune fields.|
33996|Semaphore Sand Member|73188|5|Briefly described|p320, p335|Holocene|Holocene|St Vincent Basin.||Saint Kilda Formation|||Beach sand.|
33996|Semaphore Sand Member|73236|4|Described|p36, p38, p44|Holocene|Holocene|Coastal sediments; beach and dune sands. Patchily covers the shore platform at Hallett Cove.||Saint Kilda Formation|||Lime-cemented gravel (beachrock); beach gravel of mostly quartzite pebbles to boulders; well-sorted, medium-grained quartz beach sand; well-sorted, medium-grained quartz sand of back beach dunes.|
25474|Shepparton Formation|2967|5|Briefly described|p14, p15 Fig.2.2, p18, p20 Fig.2.8, p22|Pliocene|Pliocene|Lawrence (1966). Eastern Murray Basin. Shallow aquifers. See also p28, 30-31, 33-35, 40-41, p47 Fig.2.25, p79, p83 Fig.4.5, p88, 96, 105, 128, 140, 143, 151.||Wunghnu Group.|Yando Clay Member.|Overlies Calivil Formation, Yando Clay or (in the Loddon Plain) the Parilla Sand..|Fluviolacustrine sediments: a suite of finer-grained sediments consisting of clays with interbedded shoestring sand lenses.|
25474|Shepparton Formation|10010|5|Briefly described|p12 Fig. 3|Late Pleistocene|Early Pliocene|Of the Wunghnu Group. Grades downwards into Calivil Formation. Geological Province: Murray Basin.||||||13-AUG-07
25474|Shepparton Formation|22487|6|Mentioned|p211, p212 Fig. 13|Quaternary|Tertiary|||||||11-SEP-08
25474|Shepparton Formation|22531|6|Mentioned|p6|||||||||
25474|Shepparton Formation|22756|3|Fully described|P13, P36|Pleistocene|Pliocene|||||||
25474|Shepparton Formation|22773|5|Briefly described|Fig24.8p352,354|||||||||
25474|Shepparton Formation|22782|4|Described|p16|||||||||
25474|Shepparton Formation|22799|5|Briefly described|p23 Fig.9|Late Pliocene|Late Pliocene|||||||
25474|Shepparton Formation|22857|5|Briefly described|p352-3 Figs.24.8 and 24.9, p354|Pleistocene|Late Pliocene|Of the Wunghnu Group. Fluvial and lacustrine deposits. Geological Province: Murray Basin.||||||
25474|Shepparton Formation|22886|6|Mentioned|p36|||||||||
25474|Shepparton Formation|22887|2|Defined|p45, Fig.6 p13|Pleistocene|Pleistocene|||||||
25474|Shepparton Formation|22893|3|Fully described|p61,62 table3 fig9|Pleistocene|Pleistocene|||||||
25474|Shepparton Formation|22971|4|Described|p 27||Tertiary|Max Thickness: 120m.||||||
25474|Shepparton Formation|23089|5|Briefly described|p649||Early Pliocene|||||||
25474|Shepparton Formation|23164|4|Described|p16|Pleistocene|Late Pliocene|||||||
25474|Shepparton Formation|23166|5|Briefly described|Map legend||Pliocene|||||||
25474|Shepparton Formation|23167|5|Briefly described|Map legend||Pliocene|||||||
25474|Shepparton Formation|23168|5|Briefly described|Map legend||Pliocene|||||||
25474|Shepparton Formation|23169|5|Briefly described|Map legend||Pliocene|||||||
25474|Shepparton Formation|23252|5|Briefly described|Map Legend||Pleistocene|Is subdivided into additional unnamed units.||||||
25474|Shepparton Formation|23300|5|Briefly described|Map Legend|Cenozoic|Cenozoic|||||||19-NOV-08
25474|Shepparton Formation|23302|5|Briefly described|Map Legend|Cenozoic|Cenozoic|||||||19-NOV-08
25474|Shepparton Formation|23303|5|Briefly described|Map Legend|Cenozoic|Cenozoic|||||||19-NOV-08
25474|Shepparton Formation|23304|5|Briefly described|Map Legend|Cenozoic|Cenozoic|||||||19-NOV-08
25474|Shepparton Formation|23305|6|Mentioned|p58|||Alluvium of Creswick similar to Shepparton Formation @ Kialla.||||||
25474|Shepparton Formation|23603|5|Briefly described|p12|Pleistocene|Late Pliocene|||||||
25474|Shepparton Formation|23604|5|Briefly described|Map Legend|Tertiary|Tertiary|||||||
25474|Shepparton Formation|23605|5|Briefly described|Map Legend|Tertiary|Tertiary|||||||
25474|Shepparton Formation|23606|5|Briefly described|Map Legend|Tertiary|Tertiary|||||||
25474|Shepparton Formation|23607|5|Briefly described|Map Legend|Tertiary|Tertiary|||||||
25474|Shepparton Formation|23884|5|Briefly described|p153, p155 Fig. 13.2|Pliocene|Pliocene|Geological Province: Murray Basin. Of the Wunghnu Group.||||||21-SEP-09
25474|Shepparton Formation|23921|5|Briefly described|p1109 Table 1|Quaternary|Quaternary|Geological Province: Murray Basin.||||||
25474|Shepparton Formation|24043|5|Briefly described|p525|Holocene|Pleistocene|||||||
25474|Shepparton Formation|24103|5|Briefly described|p139 Fig.3, p141|Recent|Pliocene|||||||
25474|Shepparton Formation|24106|6|Mentioned|p185|||||||||
25474|Shepparton Formation|24107|5|Briefly described|p224|Quaternary|Tertiary|||||||
25474|Shepparton Formation|24108|5|Briefly described|p241|Recent|Pliocene|Geological Province: Murray Basin. Underlying Unit: Calivil Formation.||||||29-NOV-04
25474|Shepparton Formation|24133|6|Mentioned|p51|||Geological Province: Murray Basin.||||||
25474|Shepparton Formation|24177|3|Fully described|p75, p104|Quaternary|Neogene|Overlain by the Coonambidgal Formation. Disconformably overlies the Calivil and Wild Duck Formations, White Hills Gravel and Newer Volcanics. Age: <5 Ma. Geological Province: Murray Basin.||||||11-MAY-04
25474|Shepparton Formation|24178|6|Mentioned|p18|Devonian|Ordovician|||||||
25474|Shepparton Formation|24232|5|Briefly described|p226 Fig.2, p227|||||||||
25474|Shepparton Formation|24326|5|Briefly described|Map legend|Pleistocene|Miocene|||||||
25474|Shepparton Formation|24328|5|Briefly described|Map legend|Neogene|Neogene|||||||
25474|Shepparton Formation|24329|5|Briefly described|Map legend|Neogene|Neogene|||||||
25474|Shepparton Formation|24383|5|Briefly described|p31, p40 Fig.17|Recent|Pliocene|Max Thickness: 33m. Geological Province: Lachlan Fold Belt||||||
25474|Shepparton Formation|24384|5|Briefly described|Map legend|Pliocene|Pliocene|||||||
25474|Shepparton Formation|24385|5|Briefly described|Map legend|Pliocene|Pliocene|Sandy clay and sand; fine to coarse, includes leticular gravel channel beds; red to pale cream, mottled; well to poorly sorted, unconsolidated; dissected flood plains.||||||
25474|Shepparton Formation|24386|5|Briefly described|Map legend|Pliocene|Pliocene|Sandy clay and sand: fine to coarse, includes lenticular gravel channel beds.||||||
25474|Shepparton Formation|24387|5|Briefly described|Map legend|Pliocene|Pliocene|Sandy clay and sand; fine to coarse, includes lenticular gravel channel beds.||||||
25474|Shepparton Formation|24388|5|Briefly described|Map legend|Pliocene|Pliocene|Sandy clay and sand; nonmagnetic to weakly magnetic; variable, generally low-moderate total radioelements, K, Th and U.||||||13-JUN-06
25474|Shepparton Formation|24439|5|Briefly described|p8, p37, p38|Quaternary|Cenozoic|Geological Province: Murray Basin.  see also p47 Fig. 22 Appendix 2; p60 Appendix 3.||||||19-NOV-08
25474|Shepparton Formation|24440|5|Briefly described|Map legend|||||||||
25474|Shepparton Formation|24551|5|Briefly described|p322 Fig. 10.29, p324, p731|||Of the Wunghnu Group. Maximum Thickness: 125m.||||||29-JUL-05
25474|Shepparton Formation|29591|6|Mentioned|Table 20|||||||||
25474|Shepparton Formation|29860|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
25474|Shepparton Formation|29898|4|Described|p213|||||||||
25474|Shepparton Formation|30581|6|Mentioned|Map legend|Quaternary|Quaternary|||||||
25474|Shepparton Formation|30906|6|Mentioned|Map legend|Quaternary|Quaternary|||||||
25474|Shepparton Formation|30934|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
25474|Shepparton Formation|30935|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
25474|Shepparton Formation|30936|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
25474|Shepparton Formation|31654|6|Mentioned|Map legend|Pliocene|Pliocene|||||||
25474|Shepparton Formation|31713|6|Mentioned|p4|||Also P16||||||
25474|Shepparton Formation|31742|5|Briefly described|p6|||Upper Cainozoic||||||
25474|Shepparton Formation|31746|6|Mentioned|p197|||||||||
25474|Shepparton Formation|31747|6|Mentioned|Map legend|Quaternary|Quaternary|||||||
25474|Shepparton Formation|32232|6|Mentioned|p19|||||||||
25474|Shepparton Formation|34312|5|Briefly described|p46|||Quaternary||||||
25474|Shepparton Formation|34735|4|Described|p39|||Also mention p8||||||
25474|Shepparton Formation|34757|6|Mentioned|Fig.3|||||||||
25474|Shepparton Formation|34813|6|Mentioned|p63|||||||||
25474|Shepparton Formation|34986|6|Mentioned|p339|||||||||
25474|Shepparton Formation|35091|4|Described|p11|||Also P17.||||||
25474|Shepparton Formation|35094|6|Mentioned|p12|||||||||
25474|Shepparton Formation|35111|6|Mentioned|p2|||||||||
25474|Shepparton Formation|35187|6|Mentioned|Table1|||||||||
25474|Shepparton Formation|35234|6|Mentioned|p9|||||||||
25474|Shepparton Formation|35242|6|Mentioned|p95|||||||||
25474|Shepparton Formation|35272|3|Fully described|p276|||||||||
25474|Shepparton Formation|37809|6|Mentioned|p5|||||||||
25474|Shepparton Formation|37871|4|Described|p12|||||||||
25474|Shepparton Formation|37873|6|Mentioned|p3|||||||||
25474|Shepparton Formation|37881|6|Mentioned|p16|||||||||
25474|Shepparton Formation|37882|4|Described|p6|||||||||
25474|Shepparton Formation|37883|6|Mentioned|p11|||||||||
25474|Shepparton Formation|37884|6|Mentioned|p15|||||||||
25474|Shepparton Formation|37885|5|Briefly described|p6|||||||||
25474|Shepparton Formation|38293|4|Described|p23|||||||||
25474|Shepparton Formation|39329|6|Mentioned|Fig.1|||||||||
25474|Shepparton Formation|39858|6|Mentioned|Map legend|Pleistocene|Pliocene|Pliocene - Pleistocene||||||
25474|Shepparton Formation|39860|5|Briefly described|p33|||||||||
25474|Shepparton Formation|40498|6|Mentioned|p433|||||||||
25474|Shepparton Formation|40520|6|Mentioned|Fig.5|||||||||
25474|Shepparton Formation|40522|6|Mentioned|Fig.2|||||||||
25474|Shepparton Formation|40599|5|Briefly described|p19|||||||||
25474|Shepparton Formation|40795|6|Mentioned|p80|||||||||
25474|Shepparton Formation|40820|6|Mentioned|p147|||||||||
25474|Shepparton Formation|41068|5|Briefly described|p67|||||||||
25474|Shepparton Formation|41136|5|Briefly described|p215|||||||||
25474|Shepparton Formation|41765|4|Described|p39|||||||||
25474|Shepparton Formation|41848|3|Fully described|p352||Quaternary|age ranges from approx 1 million years to 25 thousand years BP||||||
25474|Shepparton Formation|41849|6|Mentioned|p409|||Age Pleistocene||||||
25474|Shepparton Formation|41868|5|Briefly described|p551|||||||||
25474|Shepparton Formation|42125|5|Briefly described|p139|||||||||
25474|Shepparton Formation|42126|6|Mentioned|p149|||||||||
25474|Shepparton Formation|42130|6|Mentioned|Fig.3 P265|||||||||
25474|Shepparton Formation|42133|6|Mentioned|p302|||||||||
25474|Shepparton Formation|42134|4|Described|p339|||||||||
25474|Shepparton Formation|42137|5|Briefly described|p367|||See also Fig.2||||||
25474|Shepparton Formation|42138|6|Mentioned|Fig.2 P390|||||||||
25474|Shepparton Formation|42184|6|Mentioned|Fig.2 P348|||||||||
25474|Shepparton Formation|42454|4|Described|p12|Recent|Pliocene|Pliocene to 20 000BP.||||||
25474|Shepparton Formation|42455|5|Briefly described|Map legend|Recent|Pliocene|||||||
25474|Shepparton Formation|42683|5|Briefly described|map legend|||||||||
25474|Shepparton Formation|42827|3|Fully described|p352|||Of Wunghnu Group||||||13-JUN-06
25474|Shepparton Formation|42881|4|Described|Fig.3, P84|||||||||
25474|Shepparton Formation|42966|2|Defined|p187|Recent|Pliocene|Of Wunghnu Group. First published definition, but supersedes definition card.||||||13-JUN-06
25474|Shepparton Formation|43198|5|Briefly described|Map Legend|Recent|Pliocene|||||||
25474|Shepparton Formation|43199|5|Briefly described|Map Legend|Recent|Pliocene|||||||
25474|Shepparton Formation|43211|4|Described|p29||Quaternary|||||||
25474|Shepparton Formation|43218|4|Described|Fig.3,p22|Quaternary|Tertiary|||||||
25474|Shepparton Formation|43260|5|Briefly described|Map Legend|Pleistocene|Miocene|||||||
25474|Shepparton Formation|43261|5|Briefly described|Map Legend|Pleistocene|Pliocene|||||||
25474|Shepparton Formation|43493|5|Briefly described|32-36|Recent|Pleistocene|Radiocarbon dates to 30 000 years BP||||||
25474|Shepparton Formation|43578|6|Mentioned|p337|Pleistocene|Pliocene|||||||
25474|Shepparton Formation|43601|6|Mentioned|p225|||||||||
25474|Shepparton Formation|43627|6|Mentioned|p6||Quaternary|||||||
25474|Shepparton Formation|43655|5|Briefly described|p40-846|||||||||
25474|Shepparton Formation|43780|6|Mentioned|p6|||||||||
25474|Shepparton Formation|43791|6|Mentioned|p372, Fig1|||||||||
25474|Shepparton Formation|43804|6|Mentioned|Fig.2,p49|||||||||
25474|Shepparton Formation|43841|5|Briefly described|8||Tertiary|||||||
25474|Shepparton Formation|43846|5|Briefly described|14|Recent|Pleistocene|||||||
25474|Shepparton Formation|44184|5|Briefly described|Map Legend||Pleistocene|||||||
25474|Shepparton Formation|44186|5|Briefly described|Map Legend||Pleistocene|||||||
25474|Shepparton Formation|44188|5|Briefly described|Map Legend|Holocene|Pliocene|Geological province: Murray Basin. Poorly consolidated to unconsolidated mottled, variegated clay, silty clay with lenses of polymictic coarse to fine sand and gravel.||||||15-MAY-08
25474|Shepparton Formation|44197|5|Briefly described|Map Legend||Pleistocene|||||||
25474|Shepparton Formation|45168|6|Mentioned|p14|||||||||
25474|Shepparton Formation|49038|4|Described|Table 2|||Briefly described p31 and p40||||||13-JUN-06
25474|Shepparton Formation|49040|6|Mentioned|p12|||||||||
25474|Shepparton Formation|50154|2|Defined|p26, p139-140|Recent|Pliocene|Geological Province: Murray Basin. Conformably overlies the Calivil Formation. Partly equivalent to the Parilla Sand.||||||24-JUN-14
25474|Shepparton Formation|50156|5|Briefly described|Map Legend|Pleistocene|Miocene|Fluvial: prior stream, valley-backfill and floodplain deposits; clay, sand, silt, gravel.||||||
25474|Shepparton Formation|50157|5|Briefly described|Map Legend|Pleistocene|Miocene|Fluvial: prior stream, valley-backfill and floodplain deposits; clay, sand, silt, gravel.||||||
25474|Shepparton Formation|50158|5|Briefly described|Map Legend|Pleistocene|Miocene|Of Wunghnu Group. Fluvial: prior stream, valley-backfill and floodplain deposits; clay, sand, silt, gravel.||||||
25474|Shepparton Formation|50159|5|Briefly described|Map Legend|Pleistocene|Miocene|Of Wunghnu Group. Fluvial: prior stream, valley-backfill and floodplain deposits; clay, sand, silt, gravel.||||||
25474|Shepparton Formation|50160|5|Briefly described|Map Legend|Pleistocene|Miocene|Of Wunghnu Group.||||||
25474|Shepparton Formation|50161|5|Briefly described|Map Legend|Pleistocene|Miocene|Of Wunghnu Group. Fluvial: prior stream, valley-backfill and floodplain deposits; clay, sand, silt, gravel.||||||
25474|Shepparton Formation|50162|5|Briefly described|Map Legend|Pleistocene|Miocene|Of Wunghnu Formation. Fluvial: prior stream, valley-backfill and floodplain deposits; clay, sand, silt, gravel.||||||22-JUN-04
25474|Shepparton Formation|50163|5|Briefly described|Map Legend|Pleistocene|Miocene|Of Wunghnu Group. Overlies Duddo Limestone. Overlain by Lowan Sand. Fluvial: prior stream, valley-backfill and floodplain deposits; clay, sand, silt, gravel.||||||25-JUN-04
25474|Shepparton Formation|60005|5|Briefly described|Map legend|Pleistocene|Pleistocene|Fluvial: silt, sand, minor gravel.||||||11-JAN-10
25474|Shepparton Formation|60451|4|Described|p102|Holocene|Pliocene|Type section in text. Maximum Thickness: >30m. Overlies: Parilla Sand, Calivil Formation, rarely White Hills Gravel.||||||27-OCT-04
25474|Shepparton Formation|60452|4|Described|p40|Quaternary|Quaternary|Forms the flat riverine plain. Includes the Katandra, Quiamong, and Mayrung members (which probably represent only the upper part of the formation). Interfingers with Parilla Sand; disconformably overlies the Calivil Formation.||||||23-MAY-13
25474|Shepparton Formation|60454|5|Briefly described|Map Legend|Quaternary|Neogene|Dissected flood plain alluvium, terraces 1-10m above present river channels; sandy clay; fine to coarse sand; poorly sorted lenticular gravel.||||||
25474|Shepparton Formation|60456|5|Briefly described|Map Legend|Quaternary|Neogene|dissected flood plain alluvium: terraces 1-10m above present river channels; sandy clay; fine to coarse sand; poorly sorted lenticular gravel.||||||
25474|Shepparton Formation|60457|5|Briefly described|Map Legend|Quaternary|Neogene|Dissected flood plain alluvium; terraces 1-10m above present river channels; sandy clay; fine to coarse sand; poorly sorted lenticular gravel; well developed soil 2-3m thick.||||||13-JUN-06
25474|Shepparton Formation|60458|5|Briefly described|Map Legend|Quaternary|Neogene|Dissected flood plain alluvium.||||||
25474|Shepparton Formation|60461|5|Briefly described|Map legend|Recent|Miocene|Of the Murray Group.  Clay, silt, fine to coarse-grained sand of quartz, mica, feldspar and ironstone; quartz gravel.||||||06-OCT-04
25474|Shepparton Formation|60491|4|Described|p23|Quaternary|Pliocene|Overlies all units in the Charlton 1: 100K map area, except the Coonambidgal Formation, lunettes and source bordering dunes. Locally overlain by the Parilla Sand.||||||
25474|Shepparton Formation|60492|5|Briefly described|Map Legend|Pleistocene|Pliocene|Overlies the Parill Sand. Of the Wunghnu Group. Alluvium: incised floodplain deposits, prior streams and minor lake deposits; coarse grained sand, silt, clay.||||||30-SEP-04
25474|Shepparton Formation|60529|5|Briefly described|Map Legend|Recent|Pliocene|Prior stream deposits, valley backfill deposits and alluvial flood plain and swamp deposits.||||||
25474|Shepparton Formation|60591|5|Briefly described|Map Legend|Recent|Pliocene|Unconformably overlies the Mount Ida Formation, Sheoak Gully Boninite, Broadford Formation, Puckapunyal Formation and Waranga Formation.||||||
25474|Shepparton Formation|60592|5|Briefly described|Map Legend|Recent|Pliocene|Unconformably overlies the Mount Ida Formation, Sheoak Gully Boninite, Broadford Formation, Puckapunyal Formation and Waranga Formation.||||||25-NOV-04
25474|Shepparton Formation|60593|5|Briefly described|Map Legend|Recent|Pliocene|Unconformably overlies the Mount Ida Formation, Sheoak Gully Boninite, Broadford Formation, Puckapunyal Formation and Waranga Formation.||||||
25474|Shepparton Formation|60595|5|Briefly described|Map Legend|Recent|Pliocene|Unconformably overlies the Mount Ida Formation, Sheoak Gully Boninite, Broadford Formation, Puckapunyal Formation and Waranga Formation.||||||
25474|Shepparton Formation|60596|5|Briefly described|Map Legend|Recent|Pliocene|Unconformably overlies the Mount Ida Formation, Sheoak Gully Boninite, Broadford Formation, Puckapunyal Formation and Waranga Formation.||||||
25474|Shepparton Formation|60597|5|Briefly described|Map Legend|Recent|Pliocene|Nonmagnetic with dendritic, moderately magnetic responses (10-20 nT) coinciding with present and prior streams; moderate K, variable Th, and U.||||||
25474|Shepparton Formation|60599|2|Defined|p16, p24 Tb. 4, p92, p85|Recent|Pliocene|Of Wunghnu Gp. Comprises Kialla, Katandra, Quiamong + Mayrung Members, capped by Widgelli Pedoderm. Fluvial /lacustrine seds. Disconformable on Calivil + Wild Duck Fms, White Hills Gravel + Newer Volcs;overlain by Coonambidgal Formation. Murray Basin.||||||10-NOV-08
25474|Shepparton Formation|61155|5|Briefly described|p5, p18|Pleistocene|Early Pliocene|Clastics. Overlies the Calvil Formation; overlies and interfingers with Loxton-Parilla Sands. Age: <4.5Ma. Thickness: 20m. Geological Province: Murray Basin.||||||
25474|Shepparton Formation|61163|4|Described|p104-105, p36 Tb. 6.2, p177|Pleistocene|Pleistocene|Of Wunghnu Group. Overlain by Calivil Fm (also Wunghnu Gp). Geol Prov: LFB. Well-compacted channel fill conglomerate, gravel and sand, intercalated with point bar gravel and sand and finer overbank deposits - forming terrace remnants above alluvial flats.||||||06-JUL-07
25474|Shepparton Formation|61174|5|Briefly described|map legend|Quaternary |Quaternary |Of the Wunghnu Group. Clay, sand, silt, gravel: generally well sorted, well rounded; friable; polymictic; friable, deep red to pale colours. GSV map code: Nws.||||||07-FEB-11
25474|Shepparton Formation|61175|5|Briefly described|map legend|Quaternary |Quaternary |Of the Wunghnu Group. Clay, sand, silt, gravel: generally well sorted, well rounded; friable; polymictic; friable, deep red to pale colours. GSV map code: Nws.||||||
25474|Shepparton Formation|61176|5|Briefly described|map legend|Quaternary |Quaternary |Of the Wunghnu Group. Clay, sand, silt, gravel: generally well sorted, well rounded; friable; polymictic; friable, deep red to pale colours. GSV map code: Nws.||||||
25474|Shepparton Formation|61177|5|Briefly described|map legend|Quaternary |Quaternary |Of the Wunghnu Group. Clay, sand, silt, gravel: generally well sorted, well rounded; friable; polymictic; friable, deep red to pale colours. GSV map code: Nws.||||||
25474|Shepparton Formation|61178|5|Briefly described|map legend|Quaternary |Quaternary |Of Wunghnu Group. Clay, sand, silt, gravel (prior stream, valley-backfill and floodplain deposits): nonmagnetic; no discernible gravity response; low total radioelements, K moderate Th and U; low Th and high U in upper Buffalo R. GSV map code: Nws.||||||
25474|Shepparton Formation|61183|5|Briefly described|p18 Fig. 9, p68|Recent|Pliocene|Consists mostly of clay, which is mottled and contains pisolitic nodules. Geological Province: Murray Basin. See also p133. ||||||
25474|Shepparton Formation|61185|2|Defined|p63-69, p49, p53, p57|Recent|Pliocene|Incl: Kialla, Katandra, Quiamong, Mayrung Members and Widgelli Pedoderm of Wunghnu Group (Lawrence 1966). Incl: Torrumbarry Clay (Tickell 1977). Fluvial and lacustrine sediments. Overlies Strathbogie Granite and Hilldene Basalt. Underlies Coonambidgal Fm.||||||07-FEB-11
25474|Shepparton Formation|61314|5|Briefly described|p129|Quaternary|Late Pliocene|Fine-grained clastics and polymictic sands and gravels. Geological Province: eastern Murray Basin.||||||
25474|Shepparton Formation|61701|5|Briefly described|Map Legend|Recent|Pliocene|Prior stream deposits, valley backfill deposits and alluvial flood plain and swamp deposits.||||||
25474|Shepparton Formation|61702|5|Briefly described|Map Legend|Recent|Pliocene|Prior stream deposits, valley backfill deposits and alluvial flood plain and swamp deposits.||||||
25474|Shepparton Formation|61703|5|Briefly described|Map Legend|Recent|Pliocene|Prior stream deposits, valley backfill deposits and alluvial flood plain and swamp deposits.||||||
25474|Shepparton Formation|61704|6|Mentioned|Map legend|Quaternary|Quaternary|Variable radiometric respone; non-magnetic.||||||12-FEB-15
25474|Shepparton Formation|61964|3|Fully described|p14 Fig. 4, p143-144|Pleistocene|Late Pliocene|Of Wunghnu Group. Associated with Coonambidgal Fm, mapped as a Quaternary alluvial suite. Unit presents as extensive flat alluvial floodplains, traversed by traces of meandering palaeochannels. Conformably overlies Calivil Fm. Geol.Prov: Murray Basin||||||
25474|Shepparton Formation|62370|5|Briefly described|p449, p452 Fig.4|Holocene|Pliocene|Fluviolaucstrine unit which includes channel sand, levee banks of fine sandy clay and floodplain clay. Unconformably overlies Calivil Formation. Geological Province: Murray Basin. See also p464 Fig.12.||||||
25474|Shepparton Formation|62405|5|Briefly described|Map legend|Tertiary|Tertiary|Unconsolidated brown silty to sandy clay, mottled variegated clay, silty clay with sporadic lenses of polymictic fine- to coarse-gr. sand and gravel. Partly modified by pedogenesis; intercalated red-brown palaeosols.||||||25-MAR-08
25474|Shepparton Formation|63446|5|Briefly described|Map legend|Pleistocene|Pleistocene||||||Fluvial: silt, sand, minor gravel.|
25474|Shepparton Formation|63777|5|Briefly described|p1104 Fig. 1, p1105 -1108, p1110-1113|||Underlian by Calival Formation. Geological Province: Murray Basin. Series of fluvio-lacustrine clays, sands and silts.||||||
25474|Shepparton Formation|63893|5|Briefly described|p191|||Lowest units overlie Loxton-Parilla Sands and Blanchetwon Clay. Fluvial sequence generally deposited onto the erosional surface formed after the Loxton-Parilla depositional cycle.||||||
25474|Shepparton Formation|64823|5|Briefly described|p1012 Fig. 2b|Cenozoic|Cenozoic|Overlies Calivil Formation and Parilla Formation.||||||
25474|Shepparton Formation|65552|5|Briefly described|p2, p4-7, p19; p24-27 App.3-6|Holocene|Early Pliocene|Of Wanghnu Group. Hosts saline groundwater from which salt is extracted. With Coonambidgal Formation, overlies Calivil Formation and is the upper sequence in the Murray Basin. Fluvial with sporadic aeolian parna deposits and overflow lake sediments.||||||
25474|Shepparton Formation|65715|5|Briefly described|p15 Tb.8, p17|Neogene|Neogene|Of Wunghnu Group. Essentially alluvial sediments of the Murray Basin. Said to be older than Coonambidgal Formation by Lawrence (1966), but this unit no longer used by GSV.||||||
25474|Shepparton Formation|65969|5|Briefly described|p27 Tb.3.3, p30|Pliocene|Miocene|Fluvial mud and shoestring sand and gravel. Onshore sequence equivalent to Parilla Sand. Occurs in dendritic river channels draining north; fills broad topographic lows. Pliocene to Late Miocene. Streams close to basin margin have magnetic responses to 20 nT; low radiometric response.||||||
25474|Shepparton Formation|66002|5|Briefly described|p13 Tb.9, p18|Neogene|Neogene|Of Wunghnu Group. Defined by Lawrence 1966. Essentially alluvial sediments. In Murray Basin||||||
25474|Shepparton Formation|66244|6|Mentioned|p8.|||||||Overlies the Balmattum Basalt at its downstream end.||12-FEB-15
25474|Shepparton Formation|66286|5|Briefly described|p182, pp185-187, p190.|||Regarded as the source of much of the infiltrated clays and possible silts in Lithofacies D and E of Loxton-Parilla sands. 3 - 5 m thick sandy muds and sandy clays. Lacustrine and fluvial overbank sediments with channel fills.||||Overlies Loxton-Parilla sands.|Sandy clays, sandy muds, gravelly lenses with ferruginous pisoliths set in lenticular mottled clay.|
25474|Shepparton Formation|67179|4|Described|p580-85, Fig.1b, Fig.3, Fig.4|Holocene|Pliocene|May fill the the swales between Loxton Sand strandlines.||||Overlies the Loxton Sand (locally the Wandella Sandstone Member) in eastern Murray Basin, underlies the Coonambidgal Formation (conformably).|Unconsolidated to poorly consolidated clay, silt and silty clay deposited as floodplain muds, intercalated with lenses of fine to coarse sand and gravel.|
25474|Shepparton Formation|68116|5|Briefly described|Appendix, Maps 7-8, 10-26, 29-33, 42.|Holocene|Pliocene||||||Clay, sand, silt, poorly-sorted lenticular gravel. Dissected flood plain alluvium: terraces 1-10 metres above present river channels; well developed soil 2-3 m thick.|
25474|Shepparton Formation|68140|5|Briefly described|p1699, p1702, p1703 Fig.4, pp1706-1708|||Uppermost unit. Heterogeneous and laterally discontinuous. Groundwater in this unit is susceptible to contamination from human activities on the surface.||||Underlain by the Loxton-Parilla Sands. Underlain by the Calivil-Renmark Formation.|Comprises fluvio-lacustrine clays, sands and silts; laterally discontinuous.|09-FEB-18
25474|Shepparton Formation|68189|5|Briefly described|p4, p27 Tb.3.2, p29, p30, p31 Fig.16|Quaternary|Miocene|Flood plain and prior stream deposits; the flood plain deposits interfinger and overlap with the Parilla Sand.||||Conformably underlain and interfingers with the Parilla Sand.  Possibly underlain by the Blanchetown Clay.|Comprises mud and shoestring sand.|
25474|Shepparton Formation|68194|5|Briefly described|p6, p9, p11, p17, p21, p24-27, p35-36|Pleistocene|Pliocene|See also p40, p44, p56-57, p66. Lawrence (1966). Fluvio-lacustrine sediments forming flat clay plains. Regolith and remote sensing profiles described.||Unit in Wunghnu Group.||Disconformably overlies Parilla Sand.|Sands and gravels.|
25474|Shepparton Formation|69089|5|Briefly described|Map legend|Pleistocene|Pleistocene||||||Fluvial: silt, sand, minor gravel.|
25474|Shepparton Formation|69162|5|Briefly described|Map legend|Tertiary|Tertiary|Murray Basin.|||||Unconsolidated brown silty to sandy clay, mottled variegated clay, silty clay with sporadic lenses of polymictic fine- to coarse-grained sand and gravel; partly modified by pedogenesis; intercalated red-brown palaeosols.|
25474|Shepparton Formation|69163|5|Briefly described|Map legend|Tertiary|Tertiary|Murray Basin.|||||Unconsolidated brown silty to sandy clay, mottled variegated clay, silty clay with sporadic lenses of polymictic fine- to coarse-grained sand and gravel; partly modified by pedogenesis; intercalated red-brown palaeosols.|
25474|Shepparton Formation|69798|5|Briefly described|p4 Fig.2|Pliocene|Pliocene|Murray Basin.||Wunghnu Group.||||
25474|Shepparton Formation|70718|4|Described|p17, p23, p25, p104|Pliocene|Pliocene|Deposited in a fluvio-lacustrine environment with floodplain, channel and levee components and minor aeolian influences. Is one of the primary aquifers in the Hay map sheet area. Shallow aquifers in this formation have a  higher salinity in the east and pockets of lower salinity in the west; this is attributed to fresh water influx frfom the Murrumbidgee alluvial fan.||Wunghnu Group||Transitionally overlies the Calivil Formation. Overlain by the Coonambidgal Formation. Equivalent to the Parilla Sand.|Unconsolidated to poorly consolidated, mottled, variegated clay, silty clay with lenses of polymictic, coarse to fine-grained sand and gravel; partly modified by pedogenesis, includes intercalated red-brown palaeosols.|
25474|Shepparton Formation|70961|14|Not recorded|p133|||Refers to Lawrence (1966).||||||
25474|Shepparton Formation|71593|4|Described|p53-p54, p56||Pliocene|Deposited by fluvial systems. Generally less than 10-20m thick. ||||Overlies the Loxton Sand.|Laterally extensive clayey overband sediments.|
25474|Shepparton Formation|72445|5|Briefly described|App 1; App.2; App.7 p7, p7 Fig.4.|Quaternary|Pliocene|Shown on the 'Lithostratigraphy of Cenozoic sediments in the Murray Basin' (from Brown & Stephenson 1991). Described, along with Loxton-Parilla Sands, Shepparton Formation, as fluvio lacustrine. Identified in Stavely 09,10, 12, 16.||Wunghnu Group||Overlies Loxton Sand (sharp contact). Shown as overlying Calivil Formation (sharp contact) and Torrumbarry Clay partially equivalent to Wandella Limestone Member and Blanchetown Clay.|Includes mottled sandy silt; silty mud and fine sand; silty to sandy mud; muddy sand (soil horizon).|
25474|Shepparton Formation|73118|5|Briefly described|p17, 30, 34, 42, 48, 81|Quaternary|Pliocene|Murray Basin. 100m thick; generally <70m. Forms extensive flat alluvial floodplains. Drill core summary logs. Fluvio-lacustrine, flood-plain, channel and levee deposits; minor aeolian.||Wunghnu Group||Overlies Loxton-Parilla Sands, Duddo Limestone, Grampians Group.|Un- to poorly-consolidated, mottled to variegated clay, silty clay with lenses of coarse to fine polymictic sand and gravel. Forms red-brown palaeosols.|
25474|Shepparton Formation|73228|6|Mentioned|p57, p62|Quaternary|Pliocene|Underlain by an erosion or non-depositional horizon.||||Overlain by Coomandook Formation[?]. Equivalent to Bookpurnong Formation[?].||
25474|Shepparton Formation|73229|6|Mentioned|p67|||Murray Basin. Shown in Fig.1 as Miocene to Pliocene.||||||31-OCT-22
25474|Shepparton Formation|73496|5|Briefly described|Map legend|Pleistocene|Miocene|||Wunghnu Group|||Prior stream deposits and minor alluvium; mostly nonmagnetic but with dendritic, moderately magnetic responses (to 10-20 nT) coinciding with present and prior streams; high K, low Th, U radiometric highs.|
25474|Shepparton Formation|73497|5|Briefly described|Map legend|Pleistocene|Miocene|||Wunghnu Group|||Prior stream, valley-backfill and floodplain deposits: nonmagnetic with moderately magnetic responses (10-20 nT) with a dendritic pattern coinciding with drainage; low-high K, Th and U.|
25474|Shepparton Formation|73505|4|Described|p2, p11, p13|Pliocene|Late Miocene|Murray Basin. Topography of dendritic river channels draining north, fills broad lows. Low radiometric response.||Wunghnu Group||Onshore sequence equivalent of Parilla Sand, sequence/time equivalent of Bookpurnong beds and Parilla Sand|Fluvial mud and shoestring sand.|
25474|Shepparton Formation|73576|5|Briefly described|p802|Paleogene|Paleogene|Partially covers Tarnagulla Granodiorite.|||||Alluvium.|
73297|Sherbrook Supersequence|63134|2|Defined|108-110|||||||||
73297|Sherbrook Supersequence|63269|5|Briefly described|p605, p607, p609|Late Cretaceous|Late Cretaceous|Otway Basin.||||Overlies Shipwreck Supersequence. Is overlain by Wangerrip Supersequence.||
73297|Sherbrook Supersequence|69297|5|Briefly described|p78, p80, p81, p83, p98, p110, p114-p116|Late Cretaceous|Late Cretaceous|Otway Basin. Coastal plain, deltaic and marine sediments up to 5km thick. ||||||
73297|Sherbrook Supersequence|69651|5|Briefly described|p2, p10, p12, p15, p17-21, p23, p27|Late Cretaceous|Late Cretaceous|See also p31-33, p36-40, p42-43, p45-47, p49-50. Otway Basin. Campanian to Maastrichtian age. Marginal marine to fluvial deltaic (regional regression) sediments. About 900m thick. Good oil and gas potential in the Strahan Sub-basin. An excellent offshore regional seal.||||Overlies Shipwreck Supersequence. Is overlain by Wangerrip Supersequence.|Coarse-grained sandstone, breccia-conglomerate sandy shale, sandy claystone and clayey sandstone.|
73297|Sherbrook Supersequence|70077|5|Briefly described|Nelson: p1. Regional: Fig.4; p4-7, p9|Late Cretaceous|Late Cretaceous|Otway Basin. Up to 5km thick, basinward-thickening progradational succession of coastal plain, deltaic and marine sediments.||||||
73297|Sherbrook Supersequence|70078|5|Briefly described|Regional: Fig.4; p3-4, p6|Late Cretaceous|Late Cretaceous|Hosts part of Austral 3 petroleum system. Fluvio-deltaic to marine environments.||||Overlies Shipwreck Supersequence. Is overlain by Wangerrip Supersequence.||
73297|Sherbrook Supersequence|70193|5|Briefly described|p283, p284 Fig 2|Thanetian|Albian|Geological province: Otway Basin. See also Sherbrook Group.|||Includes the Paaratte Formation.|||
73297|Sherbrook Supersequence|70880|5|Briefly described|p77, 83, 85|Maastrichtian|Campanian|Otway Basin.||||Overlies Shipwreck Supersequence. Is overlain by Wangerrip Supersequence.|Major deltaic deposition.|
73297|Sherbrook Supersequence|71266|5|Briefly described|p614 Fig.3, p615|Late Cretaceous|Late Cretaceous|Otway Basin. Deltaic deposits thicken southwards.||||Overlies Shipwreck Supersequence. Is overlain by Wangerrip Supersequence.||
42216|Shipwreck Subgroup|24314|5|Briefly described|p61 Fig.2|Turonian|Cenomanian|Geological Province: Otway Basin.||||||
42216|Shipwreck Subgroup|61547|6|Mentioned|p461 Fig.2, p462. |Late Cretaceous|Late Cretaceous|||Unit in Sherbrook Group.|Includes Waarre Sandstone and Copa Formation.|||
42216|Shipwreck Subgroup|61627|5|Briefly described|p500 Fig. 2|Late Cretaceous|Late Cretaceous|Of Sherbrook Group. Includes Belfast Mudstone, Waarre Sandstone, Copa and Flaxman Formations. Geological Province: Otway Basin.||||||07-FEB-11
42216|Shipwreck Subgroup|63124|5|Briefly described|p49 Fig. 5.2|Late Cretaceous|Late Cretaceous|Of Sherbrook Group. Geological Province: Otway Basin.||||||
42216|Shipwreck Subgroup|63431|5|Briefly described|p677 Fig. 2|Turonian|Cenomanian|Of the Sherbrook Group. Includes the Copa Formation and Waarre Sandstone. Geological Province: Penola Trough/Otway Basin.||||||07-FEB-11
73296|Shipwreck Supersequence|63134|2|Defined|104-108|||||||||
73296|Shipwreck Supersequence|63269|5|Briefly described|p605, p607, p609|Late Cretaceous|Late Cretaceous|Otway Basin.||||Overlies Eumeralla Supersequence. Is overlain by Sherbrook Supersequence.||
73296|Shipwreck Supersequence|69297|6|Mentioned|p78, p81, p83, p98, p110, p114-p116|Late Cretaceous|Late Cretaceous|Otway Basin. Fluvio-lacustrine, deltaic and marine sediments. |||Includes the Waarre and Flaxman Formations.|||
73296|Shipwreck Supersequence|69651|5|Briefly described|p2, p10, p12-19, p23, p26, p31-34,p36-40|Late Cretaceous|Late Cretaceous|See also p42-47, p49-50. Otway Basin. Turonian to Santonian age. Includes the economically important reservoirs of the Waarre and Flaxman Formations, and Thylacine Member (Belfast Mudstone). Over 1300m thick (at least locally). Fluvial to deltaic and marginal marine facies. An excellent offshore regional seal. Modelling diagrams.||||Overlies Eumeralla Supersequence. Is overlain by Sherbrook Supersequence.|Basal conglomerate; interbedded sandstone, siltstone and claystone.|
73296|Shipwreck Supersequence|70077|5|Briefly described|Nelson: p1. Regional: Fig.4; p4-7, p9-10|Late Cretaceous|Late Cretaceous|Otway Basin. Includes Sherbrook Group (Waarre and Flaxman Formations). Fluvio-lacustrine, deltaic and marine sediments. Sealed by Belfast Mudstone.||||||
73296|Shipwreck Supersequence|70078|5|Briefly described|Regional: Fig.4; p3-4, p6|Late Cretaceous|Late Cretaceous|Hosts part of Austral 3 petroleum system. Fluvio-deltaic to marine environments.||||Overlies Eumeralla Supersequence. Is overlain by Sherbrook Supersequence.||
73296|Shipwreck Supersequence|70880|5|Briefly described|p76-78, 81-82|Santonian|Turonian|Otway Basin. Comprises three seismically-defined stratal units (described).||||Unconformably overlies Eumeralla Supersequence. Is overlain by Sherbrook Supersequence.||
73296|Shipwreck Supersequence|71266|5|Briefly described|p614 Fig.3|Late Cretaceous|Late Cretaceous|Otway Basin. Thickens southwards.||||Unconformably overlies Eumeralla Supersequence. Is overlain by Sherbrook Supersequence.||
70121|Silver City Suite|62728|5|Briefly described|p26|||Of Potosi Supersuite. Suite of gneisses outcropping in the Broken Hill Domain. Geological Province: Broken Hill Domain/Curnamona Province.||||||07-FEB-11
70121|Silver City Suite|62993|6|Mentioned|p37|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain.|||Includes Alma Gneiss|||15-DEC-21
70121|Silver City Suite|63866|5|Briefly described|p38, p41|||Named by Stevens (2006) to include the Alma Gneiss, Rasp Ridge Gneiss and three other newly identified magmatic units.|||Includes the Alma Gneiss, Rasp Ridge Gneiss, Georges Bore Granite, Stephens Creek Granite Gneiss and the Wondervale Well Granite Gneiss.|Intrudes the Thackaringa Group and/or the Broken Hill Group.||
70121|Silver City Suite|64097|2|Defined|p328 Appdx., p304 Fig. 1, p323|Paleoproterozoic|Paleoproterozoic|Formerly mapped in Thackaringa Gp - revised as separate suite comprising Alma, Georges Bore, Stephens Ck, Wondervale Well + Rasp Ridge Granite Gneisses -all intrude Thackaringa and/or Broken Hill Gps.Geochemically discussed as part of Potosi Supersuite||||||07-FEB-11
70121|Silver City Suite|64741|5|Briefly described|p301 Fig. 4, p302, p310|Paleoproterozoic|Paleoproterozoic|Includes Alma Gneiss, Georges Bore, Stephens Creek, Wondervale Well and Rasp Ridge Granite Gneisses. Geological province: Broken Hill Domain. Granite sills/metagranites. Peraluminous S-type.||||||07-FEB-11
70121|Silver City Suite|64944|5|Briefly described|p28 Fig. 1|Paleoproterozoic|Paleoproterozoic|Includes Alma Gneiss, Georges Bore, Stephens Creek, Wondervale Well, Rasp Ridge and unnamed dolerite sills, dykes. Age range: 1704+/-3Ma to 1683+/-3Ma. Granite sills||||||07-FEB-11
70121|Silver City Suite|66302|5|Briefly described|p35, p36 Fig.9|Statherian|Statherian|Broken Hill Domain, Curnamona Province. Formed by the melting of lower Willyama Supergroup or underlying rocks. |1705-1685 Ma||Includes the Rasp Ridge Gneiss, Georges Bore Granite, Oakdale Granite Gneiss and the Stephens Creek Granite Gneiss.|Intrudes the Thackaringa Group and Broken Hill Group.|S-type granites.|
70121|Silver City Suite|67581|6|Mentioned|p44 Fig.8, p45|||||Willyama Supergroup.||||
70121|Silver City Suite|68067|6|Mentioned|Map legend.|||Areas with higher magnetic response are mapped separately.||||||27-AUG-13
70121|Silver City Suite|68126|5|Briefly described|p26, p29-30|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain, Curnamona Province.|c.1705-1685 Ma (Stevens et al. 2008).|||||
70121|Silver City Suite|69999|6|Mentioned|p4|||||||||
70121|Silver City Suite|70000|5|Briefly described|p31, p33-34, p36-37|Statherian|Statherian|Interpreted to have acted as a thermal driver for deposition of BIF and massive Pb-Zn-Ag sulfide mineralisation.|1695-1683 Ma.|Unit in Willyama Supergroup.|Includes Alma, Georges Bore, Stephens Creek, Wondervale Well and Rasp Ridge, Granite Gneisses.|Intrudes Broken Hill Group.|Granite sills.|
70121|Silver City Suite|70015|5|Briefly described|Map legend|Statherian|Statherian|Mineral deposits (if any) are shown.||Unit in Willyama Supergroup.|Includes Alma, Georges Bore, Stephens Creek, Wondervale Well and Rasp Ridge Granite Gneisses.||Metagranitic rocks: quartz-feldspar-biotite gneiss (some megacrystic), +/- garnet, sillimanite; granitic to pegmatitic leucosome veins/patches.|17-SEP-15
70121|Silver City Suite|70657|4|Described|p12, p13 Fig.6, p15, p45|Statherian|Statherian|Stevens et al. (in prep). Curnamona Province: Broken Hill Domain.|1704 +/- 3 Ma -1683 +/- 3 Ma||Alma Gneiss, Georges Bore Granite Gneiss, Rasp Ridge Granite Gneiss, Wondervale Well Granite Gneiss, Stephens Creek Granite Gneiss.|Intrudes Broken Hill, Thackaringa Groups (Willyama Supergroup). Hores Gneiss is of similar age.|S-type felsic intrusive rocks; granite sills.|
70121|Silver City Suite|70658|5|Briefly described|p2, 15|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain, Curnamona Province. Result of melting of lower part of rift in-fill.|~1705-1685 Ma.||Alma Gneiss.|Associated with Thackaringa and Broken Hill Groups.|Granite sills.|
70121|Silver City Suite|71968|6|Mentioned|p4|||Geological province: Curnamona province.||||||
70121|Silver City Suite|73030|6|Mentioned|p2150|Statherian|Statherian||ca. 1700-1680|||||
70121|Silver City Suite|73243|6|Mentioned|p53 Fig.2||||||||Meta-granites.|
70121|Silver City Suite|73482|5|Briefly described|p422 Fig.3||||||Rasp Ridge Granite Gneiss, Wondervale Well Granite Gneiss, Stephens Creek Granite Gneiss, Georges Bore Granite Gneiss|||
70121|Silver City Suite|73512|5|Briefly described|p2-3|Statherian|Statherian|Curnamona Province, Broken Hill Block. Emplaced at ca 1700-1685 Ma.|ca 1704-1683 Ma||||Includes Potosi-type gneisses, and granitic rocks.|
70121|Silver City Suite|73524|5|Briefly described|p3|Statherian|Statherian|Proposed to have been emplaced during early rifting/basin opening.|1705-1685 Ma||Alma Gneiss, Rasp Ridge Gneiss|Intrudes lower Willyama Supergroup|Granitic sills, metamorphosed.|
70121|Silver City Suite|73575|5|Briefly described|p826, p828 Fig.2, p829 Fig.3|||||||Alma Granite Gneiss, Georges Bore Granite Gneiss, Stephens Creek Granite Gneiss, Wondervale Well Granite Gneiss, Rasp Ridge Granite Gneiss|Granite gneiss sills.|
24496|Six Mile Bore Member|40672|2|Defined|p2|Early Cambrian|Early Cambrian|of Parara Limestone.||||||
24496|Six Mile Bore Member|40831|6|Mentioned|p5|||||||||
24496|Six Mile Bore Member|42226|4|Described|p232|||||||||
24496|Six Mile Bore Member|44133|5|Briefly described|p23|||Of the lower Mernmerna Formation. (Clarke 1986)||||||
24496|Six Mile Bore Member|60418|5|Briefly described|p135|Botoman-Atdabanian|Botoman-Atdabanian|Thickness: 207m. Interbedded dark grey to black nodular dolomitic limestones and shales. Of Mernmerna Formation.||||||
24496|Six Mile Bore Member|62784|6|Mentioned|p9|Early Cambrian|Early Cambrian|Unit in lower Mernmerna Formation of Hawker Group, Arrowie Basin.||||||
24496|Six Mile Bore Member|63569|6|Mentioned|p119|Early Cambrian|Early Cambrian|||Unit in lower Mernmerna Formation.||||
24496|Six Mile Bore Member|70833|5|Briefly described|p186,188,198,200|Series 2|Series 2|Of Arrowie Basin. Key section: 10MS-W (Ten Mile South, SE Bunkers Graben). ||Unit of Mernmerna Formation.||Uppermost unit of Mernmerna Formation. Underlain by Linns Springs Member.||
24496|Six Mile Bore Member|70835|6|Mentioned|p336|Cambrian|Cambrian|Arrowie Basin, Flinders Ranges.||Mernmerna Formation.||Unconformably overlies Winnitinny Creek Member (Wilkawillina Limestone). Is overlain by Linns Springs Member.||
24496|Six Mile Bore Member|71102|5|Briefly described|p246,251|Series 2|Series 2|Of Arrowie Basin. Nomenclature of Clarke (1986b, 1990a) in the Bunkers Graben and Range; variably developed in the Arrowie Basin. Intersected sections: DBS (Donkey Bore Syncline), MMF (Bunkers Range, Central Flinders Ranges), 10MS (10 Mile South, Bunkers Graben). Variably developed within the Arrowie Basin.||Unit of Mernmerna Formation.||Overlain by Linns Springs Member.||
25481|Skillogalee Dolomite|9862|6|Mentioned|Map Legend|Adelaidean|Adelaidean|named used as an equivalent.||||||
25481|Skillogalee Dolomite|22505|5|Briefly described|p7||Neoproterozoic|||||||
25481|Skillogalee Dolomite|22589|6|Mentioned|p129||Cryogenian|||||||
25481|Skillogalee Dolomite|22772|5|Briefly described|Table13.1|Cryogenian|Cryogenian|||||||
25481|Skillogalee Dolomite|22802|6|Mentioned|p871|||Burra Group||||||
25481|Skillogalee Dolomite|22857|5|Briefly described|Tb. 13.1 (insert p70-71)|Torrensian|Torrensian|Of the Mundallio Subgroup (Burra Group).||||||
25481|Skillogalee Dolomite|22869|5|Briefly described|p37, p39, Table2|||||||||17-SEP-19
25481|Skillogalee Dolomite|22889|4|Described|p34|Adelaidean|Adelaidean|Of the Mundallio Subgroup.||||||11-SEP-07
25481|Skillogalee Dolomite|22926|6|Mentioned|42|||Geol province Adelaide Geosyncline||||||
25481|Skillogalee Dolomite|23054|5|Briefly described|p11-2|||||||||
25481|Skillogalee Dolomite|23287|6|Mentioned|p102|||Eastern Margin of Stuart Shelf.||||||
25481|Skillogalee Dolomite|23288|6|Mentioned|p143 Fig.18|||equivalent of Loves Creek Member. Of Burra Group, Adelaide Geosyncline.||||||
25481|Skillogalee Dolomite|23314|5|Briefly described|331 Fig.2|||||||||
25481|Skillogalee Dolomite|23315|6|Mentioned|p344|Neoproterozoic|Neoproterozoic|Of the Burra Group.||||||07-FEB-07
25481|Skillogalee Dolomite|23394|5|Briefly described|Map legend|Proterozoic|Proterozoic|||||||
25481|Skillogalee Dolomite|23411|6|Mentioned|Map Legend|||||||||
25481|Skillogalee Dolomite|23482|6|Mentioned|p9|||||||||
25481|Skillogalee Dolomite|23557|5|Briefly described|p96 Fig.2|||Geological Province: Adelaide Rift Complex.||||||
25481|Skillogalee Dolomite|23719|5|Briefly described|p25|Neoproterozoic|Neoproterozoic|Underlain by Burra Group rocks. Geological Province: Gawler Craton. Max. thickness >300 m.||||||11-SEP-07
25481|Skillogalee Dolomite|23731|6|Mentioned|p12|Neoproterozoic|Neoproterozoic|||||||
25481|Skillogalee Dolomite|23869|6|Mentioned|p16|||||||||
25481|Skillogalee Dolomite|24175|3|Fully described|p11|Neoproterozoic|Neoproterozoic|Of Mundallio Subgroup (Burra Group). Conformably overlain by Myrtle Springs Formation; conformably underlain by Witchelina Quartzite. Max. thickness: 4000m.||||||13-FEB-08
25481|Skillogalee Dolomite|24176|4|Described|p10, p25 Tb. 1|Adelaidean|Adelaidean|Of Burra Gp.  Dolomites, magnesite, chert; stromatolites; in Mt. Painter Prov. these are metamorphosed to an assemblage of tremolite-actinolite rocks.  Max. thickness: 1740m.  Overlain by Myrtle Springs Formation.  Geol. Prov.: Mount Painter Province.||||||
25481|Skillogalee Dolomite|24283|5|Briefly described|p13|||||||||
25481|Skillogalee Dolomite|24321|5|Briefly described|Map legend|Adelaidean|Adelaidean|Parent: Mundallio Subgroup||||||
25481|Skillogalee Dolomite|24506|5|Briefly described|p18 Fig. 4, p19 Fig. 5|Neoproterozoic|Neoproterozoic|Parts preserved in synclinal cores.  Overlies Mount  Margaret  Quartzite.||||||
25481|Skillogalee Dolomite|24546|5|Briefly described|p2 - 3 Fig.2|Neoproterozoic|Neoproterozoic|Of Burra Group. Overlain by Undalya Quartzite. Geological Province: Adelaide Fold Belt.||||||16-JAN-08
25481|Skillogalee Dolomite|24593|5|Briefly described|p613 Fig. 1b|||Of the Burra Group.  Geological Province: Mount Painter Inlier.||||||
25481|Skillogalee Dolomite|29780|4|Described|p21|||||||||
25481|Skillogalee Dolomite|30052|6|Mentioned|Fig.6|||Proterozoic age.||||||
25481|Skillogalee Dolomite|30176|6|Mentioned|Map legend|Adelaidean|Adelaidean|Torrensian||||||
25481|Skillogalee Dolomite|30177|4|Described|p164|||See also p273.||||||11-SEP-07
25481|Skillogalee Dolomite|30801|6|Mentioned|p5|||Burra Group. Table p5-6||||||18-JAN-19
25481|Skillogalee Dolomite|30802|4|Described|Table 1|||Torrensian age.See also p7.||||||11-SEP-07
25481|Skillogalee Dolomite|30807|6|Mentioned|p103|||Suggested map symbol||||||
25481|Skillogalee Dolomite|30918|6|Mentioned|p80|||||||||
25481|Skillogalee Dolomite|31022|4|Described|Fig. 3|||See also Fig. 4. Unit of Burra Group.||||||11-SEP-07
25481|Skillogalee Dolomite|31155|6|Mentioned|p111|||[Originally entered for Tas. CEBMar95]||||||
25481|Skillogalee Dolomite|31292|6|Mentioned|p3|||||||||
25481|Skillogalee Dolomite|32032|6|Mentioned|p7|||Unit of Burra Group. See also Fig.2.||||||
25481|Skillogalee Dolomite|32508|6|Mentioned|p119|||||||||
25481|Skillogalee Dolomite|32720|6|Mentioned|p7|||Age 1000 my.||||||
25481|Skillogalee Dolomite|32721|6|Mentioned|p82|||Burra Gp.||||||
25481|Skillogalee Dolomite|32722|6|Mentioned|Fig.3|||Adelaidean. Stromatolite||||||
25481|Skillogalee Dolomite|32724|4|Described|p503|||See also p504-508. Torrensian.||||||11-SEP-07
25481|Skillogalee Dolomite|32725|6|Mentioned|p3|||Stratigraphy||||||
25481|Skillogalee Dolomite|32726|6|Mentioned|p200|||Preservation of stromatolite structures||||||
25481|Skillogalee Dolomite|32727|6|Mentioned|p13|||||||||
25481|Skillogalee Dolomite|33026|6|Mentioned|p537|||||||||
25481|Skillogalee Dolomite|33474|6|Mentioned|Fig.4|||||||||
25481|Skillogalee Dolomite|33956|4|Described|p1040|||||||||
25481|Skillogalee Dolomite|34202|6|Mentioned|p1057|||Burra Group. p1058.||||||18-JAN-19
25481|Skillogalee Dolomite|34268|6|Mentioned|p241|||U.Prot.||||||
25481|Skillogalee Dolomite|34269|6|Mentioned|Table 1|||||||||
25481|Skillogalee Dolomite|34320|6|Mentioned|Fig.|||Regional geology plan.||||||
25481|Skillogalee Dolomite|34483|5|Briefly described|p111|||Torrensian. Corr. with Bitter Springs Formation. See also pp112,113,114||||||17-SEP-19
25481|Skillogalee Dolomite|34521|5|Briefly described|p156|||Suitability for road making.||||||13-FEB-08
25481|Skillogalee Dolomite|34535|4|Described|p59|||Early Torrensian. See also Fig.19 and p55.||||||11-SEP-07
25481|Skillogalee Dolomite|34536|6|Mentioned|Map legend|Adelaidean|Adelaidean|Torrensian||||||
25481|Skillogalee Dolomite|34587|5|Briefly described|p36|||||||||
25481|Skillogalee Dolomite|34615|6|Mentioned|p6|||||||||
25481|Skillogalee Dolomite|34686|6|Mentioned|p219|||||||||
25481|Skillogalee Dolomite|34959|6|Mentioned|p283|||||||||
25481|Skillogalee Dolomite|35003|6|Mentioned|p122|||||||||
25481|Skillogalee Dolomite|35090|6|Mentioned|Fig.1|||||||||
25481|Skillogalee Dolomite|35255|6|Mentioned|p13|||||||||
25481|Skillogalee Dolomite|35270|6|Mentioned|Fig.3|||||||||
25481|Skillogalee Dolomite|35328|6|Mentioned|p9|||Stratigraphy||||||
25481|Skillogalee Dolomite|35904|6|Mentioned|p6|||||||||
25481|Skillogalee Dolomite|36626|6|Mentioned|p70|||||||||
25481|Skillogalee Dolomite|36731|6|Mentioned|p123|||||||||
25481|Skillogalee Dolomite|36733|3|Fully described|p40|||||||||
25481|Skillogalee Dolomite|36839|6|Mentioned|p61|||||||||
25481|Skillogalee Dolomite|37371|6|Mentioned|p377|||||||||
25481|Skillogalee Dolomite|37461|4|Described|p337|||See also Table 5.I.||||||11-SEP-07
25481|Skillogalee Dolomite|37854|6|Mentioned|p14|||||||||
25481|Skillogalee Dolomite|37933|6|Mentioned|p552|||||||||
25481|Skillogalee Dolomite|38157|6|Mentioned|Table 1|||See also Table III and p287.||||||18-JAN-19
25481|Skillogalee Dolomite|38926|4|Described|p29|||See also p25.||||||11-SEP-07
25481|Skillogalee Dolomite|39210|6|Mentioned|Table 3|||||||||
25481|Skillogalee Dolomite|39348|6|Mentioned|Map legend|Adelaidean|Adelaidean|Torrensian||||||
25481|Skillogalee Dolomite|39349|6|Mentioned|Map legend|Adelaidean|Adelaidean|Torrensian||||||
25481|Skillogalee Dolomite|39350|6|Mentioned|Map legend|Adelaidean|Adelaidean|Torrensian||||||
25481|Skillogalee Dolomite|39351|6|Mentioned|Map legend|Adelaidean|Adelaidean|Torrensian||||||
25481|Skillogalee Dolomite|39352|6|Mentioned|Map legend|Adelaidean|Adelaidean|Torrensian||||||
25481|Skillogalee Dolomite|39404|6|Mentioned|Map legend|Adelaidean|Adelaidean|Torrensian||||||
25481|Skillogalee Dolomite|39490|6|Mentioned|Fig.1(6)|||||||||
25481|Skillogalee Dolomite|39635|6|Mentioned|Fig.2|||||||||
25481|Skillogalee Dolomite|39866|6|Mentioned|Table 2|||||||||
25481|Skillogalee Dolomite|40225|5|Briefly described|Map sheet|||Mention Map sheet||||||
25481|Skillogalee Dolomite|40294|3|Fully described|p35|||See also p9.||||||11-SEP-07
25481|Skillogalee Dolomite|40442|6|Mentioned|Fig.2|||||||||
25481|Skillogalee Dolomite|40456|6|Mentioned|Fig.2|||||||||
25481|Skillogalee Dolomite|40500|5|Briefly described|Fig.2|||||||||
25481|Skillogalee Dolomite|40501|6|Mentioned|p115|||||||||
25481|Skillogalee Dolomite|40674|6|Mentioned|p14|||||||||
25481|Skillogalee Dolomite|40695|4|Described|p3|||||||||
25481|Skillogalee Dolomite|40852|5|Briefly described|p27|||||||||
25481|Skillogalee Dolomite|40856|5|Briefly described|p312|||||||||
25481|Skillogalee Dolomite|40985|6|Mentioned|p403|||||||||
25481|Skillogalee Dolomite|41256|5|Briefly described|p7|||See also Fig.4||||||
25481|Skillogalee Dolomite|41400|6|Mentioned|p27|||||||||
25481|Skillogalee Dolomite|41403|6|Mentioned|p49|||||||||
25481|Skillogalee Dolomite|41404|3|Fully described|p99|||||||||
25481|Skillogalee Dolomite|41405|6|Mentioned|p126|||See also Fig.50||||||
25481|Skillogalee Dolomite|41494|6|Mentioned|p32|||||||||
25481|Skillogalee Dolomite|41526|6|Mentioned|p20|||||||||
25481|Skillogalee Dolomite|42094|6|Mentioned|p20|||||||||
25481|Skillogalee Dolomite|42098|6|Mentioned|p51|||||||||
25481|Skillogalee Dolomite|42101|6|Mentioned|p84|||||||||
25481|Skillogalee Dolomite|42167|5|Briefly described|p118|||See also Fig.2||||||
25481|Skillogalee Dolomite|42222|4|Described|p13|||||||||
25481|Skillogalee Dolomite|42235|4|Described|p134|||See also Fig.3||||||
25481|Skillogalee Dolomite|42236|5|Briefly described|p107|||See also Fig.3||||||
25481|Skillogalee Dolomite|42237|4|Described|p85|||See also Fig.2||||||
25481|Skillogalee Dolomite|42238|5|Briefly described|p73|||||||||
25481|Skillogalee Dolomite|42272|6|Mentioned|p402|||||||||
25481|Skillogalee Dolomite|42505|6|Mentioned|Map legend|Adelaidean (Torrensian)|Adelaidean (Torrensian)|||||||
25481|Skillogalee Dolomite|42506|6|Mentioned|Map legend|Adelaidean (Torrensian)||||||||
25481|Skillogalee Dolomite|42720|5|Briefly described|map legend|Torrensian||||||||
25481|Skillogalee Dolomite|42733|5|Briefly described|map legend|Adelaidean||||||||
25481|Skillogalee Dolomite|42760|4|Described|p2|||||||||
25481|Skillogalee Dolomite|42761|4|Described|p5|||see also Fig.2 p8, Fig.3 p10||||||11-SEP-07
25481|Skillogalee Dolomite|42813|5|Briefly described|p16|||Of the Burra Group.||||||11-SEP-07
25481|Skillogalee Dolomite|43052|5|Briefly described|p179,Table 6.1|||Of Mundallio Subgroup.||||||16-SEP-08
25481|Skillogalee Dolomite|43057|6|Mentioned|Fig.2.24|||of Burra Group||||||
25481|Skillogalee Dolomite|43742|6|Mentioned|Fig.4,p42||Neoproterozoic|||||||
25481|Skillogalee Dolomite|43845|5|Briefly described|Fig3 p4,; 44||Neoproterozoic|In Burra Group||||||12-JUL-16
25481|Skillogalee Dolomite|44133|5|Briefly described|p53, 57|Adelaidian|Adeladian|Mineralised and hydrothermally altered.||||||
25481|Skillogalee Dolomite|44289|5|Briefly described|Map Legend||Neoproterozoic|||||||
25481|Skillogalee Dolomite|44659|5|Briefly described|map legend|||Torrensian, lithology.||||||
25481|Skillogalee Dolomite|44660|14|Not recorded|map legend|||Torrensian, lithology.||||||
25481|Skillogalee Dolomite|44689|14|Not recorded|map legend|||Andamooka. (H53-12). (Equivalent).||||||
25481|Skillogalee Dolomite|44690|4|Described|map legend|||Geol. Atlas Series. (I/54-5). Unit of Burra Group. Torrensian.||||||
25481|Skillogalee Dolomite|46861|6|Mentioned|p9|||||||||
25481|Skillogalee Dolomite|50327|5|Briefly described|p306|Torrensian|Torrensian|Within the Adelaide Rift Complex of South Australia. References to correlations with Tasmanian units.||||||07-FEB-11
25481|Skillogalee Dolomite|60718|5|Briefly described|p49, 52, 55|Adelaidean|Adelaidean|Max. thickness: nearly 4000m. Geological Province: Adelaide Geosyncline. Peritidal carbonate succession. See also p51 Fig. 3. Mined for magnesite.||Of Mundallio Subgroup (Burra Group).||Passes down into Witchelina Quartzite.||15-APR-11
25481|Skillogalee Dolomite|60959|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Of the Mundallio Subgroup. Grey-green siltstone, dolomite, sandstone, chert, conglomerate.||||||
25481|Skillogalee Dolomite|61307|5|Briefly described|p25 Fig. 14|Torrensian|Torrensian|Of the Burra Group. Geological Province: Adelaide Fold Belt.||||||
25481|Skillogalee Dolomite|61523|5|Briefly described|p12|Adelaidean|Adelaidean|Geological Province: Mount Painter Province.||||||
25481|Skillogalee Dolomite|62592|5|Briefly described|p50 Table 5.1, p57.|Torrensian|Torrensian|Adelaide Geosyncline. Produces dominant seismic reflections.||Unit in Mundallio Subgroup.||Is unconformably overlain by Yudnamutana Subgroup.||
25481|Skillogalee Dolomite|62724|5|Briefly described|p17 Fig. 4|Torrensian|Torrensian|Of the Mundallio Subgroup (Burra Group). Conformably overlies River Wakefield Formation; overlain by Bungarider Subgroup rocks.||||||07-FEB-11
25481|Skillogalee Dolomite|63102|6|Mentioned|p47|||Of Adelaide Geosyncline.||||||
25481|Skillogalee Dolomite|63250|6|Mentioned|p6|||Possibly correlates with Black River Dolomite. SA unit (?)||||||
25481|Skillogalee Dolomite|63397|6|Mentioned|p10|||||||||
25481|Skillogalee Dolomite|63489|5|Briefly described|Map legend|Adelaidean|Adelaidean|Pale and dark grey dolomite, siltstone and sandstone, magnesite conglomerate.||||||11-SEP-07
25481|Skillogalee Dolomite|64769|6|Mentioned|p27|Neoproterozoic|Neoproterozoic|SA.||||||06-MAY-09
25481|Skillogalee Dolomite|64793|5|Briefly described|p284 fig 3, p285 fig 4, p290, p295|Neoproterozoic|Neoproterozoic|Adelaide Rift Complex.||Burra Group||Correlated with upper part of Kanpa Formation.||
25481|Skillogalee Dolomite|64796|5|Briefly described|p183 fig 2, p188 fig 6, p191 Fig.9 |Neoproterozoic|Neoproterozoic|See also p192, p193, p196-198 Tb.4-6, p200 Fig.10, p202-206. Does not correlate with itself between Peake & Denison Ranges and Flinders Ranges (p202). Of Adelaide Rift Complex. Very shallow marine rocks, with numerous intertongues of sand and silt from prograding deltaic front. Mis-spelt as Sillogale in Tb.5.|Maximum c.770 Ma (after Preiss, 2000).|Burra Group||Overlies Bungaree Quartzite and Mount Margaret Quartzite. Is overlain by Undalya Quartzite.|Carbonate rocks; sandstone, siltstone; sedimentary magnesite.|
25481|Skillogalee Dolomite|64797|6|Mentioned|p160 Fig.8, p161 Tb.4|||S-isotope data.||Unit in Burra Group.||||
25481|Skillogalee Dolomite|64801|5|Briefly described|p110|Neoproterozoic|Neoproterozoic|Restricted marine sedimentation with non-marine lagoonal intercalations.||Burra Group.|||Distinctive unit with common, widespread beds of magnesite intraclast conglomerate.|
25481|Skillogalee Dolomite|65365|6|Mentioned|p7|||||||||19-MAR-12
25481|Skillogalee Dolomite|65379|5|Briefly described|p643, p644|Neoproterozoic|Neoproterozoic|Of Burra Group (Warrina Supergroup). Dolomite; marble. N.B.  Asbestos deposit host, contains Hallelujah Hills and Robertstown asbestos prospects; Mt Fox asbestos occurrence, and the Blue Hole and Ruedigers asbestos mines.||||||
25481|Skillogalee Dolomite|65925|5|Briefly described|p124 Fig.3, Appendix 2.|||||Unit in Burra Group.|||Siltstone, sandstone, dolomite; dolomite and magnesite in upper levels.|
25481|Skillogalee Dolomite|66522|3|Fully described|pp19-25, pp28-30.|Neoproterozoic|Neoproterozoic|Adelaide Geosyncline. Intrusions formed diapirs of brecciated sediments. A halo of intense hydrothermal alteration, including epigenetic copper mineralisation, lies adjacent to felsic porphyry lenses. SeeLA- ICPMS dating of volcaniclastic siltstone in Kooringa Member (288+/-7 Ma).||Unit in Burra Group.|Includes Kooringa Member.|Disconformably onlaps the Rhynie Sandstone. Is overlain, with a variably-eroded surface, by the Bungarider Subgroup.|Upper unit: dark grey dolomite with black carbonaceous chert. Lower unit: cream to light grey, micritic or cryptomicrobially laminated to stromatolitic dolomite; pale diagenetic chert blebs and lenses. Local basal limestone and siltstone interbeds.|17-SEP-19
25481|Skillogalee Dolomite|66884|1|Redefined|p36-39, p41-44, incl Figs.2-4|||Revised definition. Age: middle Torrensian. Measured stratigraphic sections in Willouran Ranges (Belperio, 1987). Type locality: 460 km to south of eastern Willouran Ranges near Auburn (Thompson et al. 1964) characterised by pale grey dolomite and brown sandy dolomite. Thickness: up to 2510 m.||Mundallio Subgroup|Camel Flat Shale Member, Twenty Mile Hill Member, Old Mount North West Member|Is conformably overlain by lower member of Myrtle Springs Formation.|Dolomitic and siliciclastic sandstones and siltstones, cryptomicrobial laminated and stromatolitic beds and intraclastic dolomite and magnesite beds.|
25481|Skillogalee Dolomite|68207|6|Mentioned|p766, 768-769|||Mentioned in a graph showing Raman spectra of kerogen comprising Precambrian permineralised microfossils; demonstrating they are not merely graphite.|c.760 Ma.||||Contains Precambrian microfossils in chert.|
25481|Skillogalee Dolomite|68270|5|Briefly described|p683|Tonian|Tonian|Adelaide Rift Complex. 797+\-5 Ma (Drexel 2008).||Unit of Burra Group.||||
25481|Skillogalee Dolomite|68271|5|Briefly described|p696|||Adelaide Rift Complex. U-Pb zircon age of 794+\-4 Ma indicating minimum time of deposition (Preiss et al. 2009).||Unit of Burra Group.||||
25481|Skillogalee Dolomite|69019|4|Described|p39-41, p47, p135, p135 Fig.30, p143.|Neoproterozoic|Neoproterozoic|Forbes (1960, 1961) and several others. Hearon et al. (2010) have added 3 new named Members which are not mentioned on the Map. Thickness from 800 m to 4,000 m. Forms rugged topography. Age from a penecontemporaneous porphyry within the unit in the Burra Copper Mines. Hosts abundant dolomite and sub-economic magnesite.|c.790 Ma (U-Pb zircon; Drexel 2008).|||Conformably overlies Witchelina Quartzite. Is overlain unconformably by Tapley Hill Formation.|Lower unit: pale to white dolomite with minor quartzite (meta-sandstone) and grey slate; upper unit: dark grey to black fine-grained dolomite with fragmental magnesite, stromatolites and cryptalgal lamination.|
25481|Skillogalee Dolomite|69873|5|Briefly described|p82|||Adelaide Rift Complex. Included in diagram showing Cryogenian-Ediacaran stratigraphy and correlations with Tasmanian succession.|c.790 Ma (Preiss et al., 2009).|Unit in Burra Group.||||
25481|Skillogalee Dolomite|70384|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Adelaide Geosyncline. Shallow-marine to lagoonal deposits. Mapped as an undifferentiated unit, and lower and upper parts/members separately. The lower part forms prominent outcrops. Age shown more specifically as Torrensian [Cryogenian]. U-Pb zircon age from coeval porphyry.|~790 Ma.|Mundallio Subgroup.|||Lower part: pale hued to white dolomite; minor quartzite and slate, interbedded with minor tuffaceous units, grits, rhyolites and rhyolitic tuffs. Upper part: dark grey, fine-grained dolomite with ripple marks, slumps and mudcracks.|18-JAN-19
25481|Skillogalee Dolomite|70405|6|Mentioned|p50, p51 table 4|Neoproterozoic|Neoproterozoic|||Mundallio Subgroup|||Dolomites.|
25481|Skillogalee Dolomite|70657|6|Mentioned|p54|||Folded Adelaidean metasediments.||||||
25481|Skillogalee Dolomite|70819|6|Mentioned|p11, 13, 18|Neoproterozoic|Neoproterozoic|Clare Valley. Marginal marine to partly lacustrine.|c.790 Ma.|Mundallio Subgroup.||Overlies/is faulted against Rhynie Sandstone. Is overlain by Undalya Quartzite and Woolshed Flat Shale.||
25481|Skillogalee Dolomite|71237|14|Not recorded|p9, 18|||||||||
25481|Skillogalee Dolomite|71240|2|Defined|p6, p9-10, p18|||||||Correlated with Montacute Dolomite, Castambul Dolomite.||
25481|Skillogalee Dolomite|71711|6|Mentioned|p401, p402 Fig 10|Tonian|Tonian|Previously correlated to Black River Dolomite by Calver 1998. Revised age of the base of Togari Group (Forest Conglomerate 730 Ma; Mulder et al., 2018) does not support the correlation of the Black River Dolomite and Skillogalee Dolomite.|790 Ma|Of middle Burra Group||||
25481|Skillogalee Dolomite|72238|5|Briefly described|p42|Tonian|Tonian|Of Adelaide Geosycline. Contains volcanics dated as 788+\-7 Ma (Preiss, Drexel and Reid 2009).||||||
25481|Skillogalee Dolomite|72456|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Marree 1:250k map sheet. |||||Dolomite, marble with magnesite mud-pellet conglomerates.|
25481|Skillogalee Dolomite|72601|6|Mentioned|p6||Tonian|Geochronologic constraint by Preiss et al. (2009). Conflicted with age of the underlying Boucaut Volcanics; however, the latter age was later considered unreliable by Fanning and Link (2008).|795 +/- 5 Ma LA ICP MS|||||
25481|Skillogalee Dolomite|73086|6|Mentioned|p57|Tonian|Tonian|Penecontemporaneously intruded by a 795 +/- 6 Ma (LA-ICP-MS) porphyry.|ca 795 Ma|||||
25481|Skillogalee Dolomite|73093|5|Briefly described|map legend|Neoproterozoic|Neoproterozoic||||||White to dark grey dolomite, minor quartzite, slate and tuffaceous siltstone.|09-DEC-21
25481|Skillogalee Dolomite|73110|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic||||||Dolomite; marble, with magnesite mud-pellet conglomerates.|
25481|Skillogalee Dolomite|73188|6|Mentioned|p315, p340, p354|Tonian|Tonian|Normally the oldest unit exposed in anticlinal cores east of the Clare-Spalding Fault.|ca 790 Ma[?]||||Includes dolomitic marble.|
25481|Skillogalee Dolomite|73262|6|Mentioned|p582, p586-587|Tonian|Tonian|Adelaide Superbasin. Geochron from Lloyd et al. (2020) is a maximum depositional age. Possibly correlates to Black River Dolomite (Calver, 1998); however, detrital provenance studies show otherwise (Mulder et al., 2018).|787 +/- 9 Ma||Kooringa Member|||30-JAN-23
25481|Skillogalee Dolomite|74367|5|Briefly described|p7 Fig.6, p8-9, p13-14, p18, p20, p22-23|Tonian|Tonian|See also p11.|789+/-9 Ma LA-ICP-MS zircon|Mundallio Subgroup|Kooringa Member|||
82222|Skuse Hill Metapyroxenite|73230|1|Redefined|p6, p10, p12-13, p15-16|Siderian|Siderian|Redefined name [see appendix and ASUD for definition]; formerly Blackfellow Hill Pyroxenite. Gawler Craton. Domain: Christie and Wilgena. Concordant with carbonate and iron formation and paragneiss. Traces of nickel-copper sulfide mineralisation; contains accessory sulfide and elevated nickel and chromium contents. Metamorphism at c. 2435-2425 Ma. Interpreted to be a layered mafic complex (Daly and van der Stelt, 1992). Named after Skuse Hill on the TARCOOLA mapsheet. Type locality: drillhole Blackfellow Hill 1 (3243), interval 86-170 m (total depth). Reference drillhole: Skuse Hill 2 (3242), interval 18-76 m. Occurs in drillholes near Skuse Hill in the southern Christie Domain. Thickness: intersections in reference drillhole are up to 58 m thick but significantly less in other drillholes. Age (c. 2460 Ma) is zircon SHRIMP U-Pb from Fanning et al. (2007). Potential correlative of Aristarchus Metaperidotite.|c. 2460 Ma (magmatic)|Mulgathing Complex||Intrudes Christie Gneiss.|Garnet-bearing mafic gneiss, metagabbro, metapyroxenite and metanorite.|
73491|Skylark Metasediments|66302|6|Mentioned|p20, p32|||Mount Woods Domain, Gawler Craton. Maximum depositional ages. Ages from Jagodzinski et al. (2007) and Chalmers (2007) respectively.|1752 +/- 6 to 1749 +/- 6 Ma (SHRIMP U-Pb)|Mount Woods Complex||Unconformably overlain by the Coodnambana Metaconglomerate.||05-SEP-22
73491|Skylark Metasediments|71341|6|Mentioned|p187 fig 6|||||||||
73491|Skylark Metasediments|73155|4|Described|p263, p265-269, p274-275, p277, p279-287|Statherian|Statherian|Gawler Craton, Mount Woods Domain, southern and western. 1755+/-10 Ma zircon age interpreted as maximum depositional age, 1641+/-23 Ma zircon age is a possible age for metamorphism. 1736+/-14 Ma zircon U-Pb interpreted to constrain high-temperature metamorphism (Daly et al., 1998). Contact with Engenina Adamellite and Balta Granite at Moonlight Shear Zone. May be part of same stratigraphic package as Blue Duck Group and Kennedy's Dam Group, may be broad equivalence between them. Interpreted as part of hangingwall/upper plate of Mount Woods Metamorphic Core Complex. Misspelt as Syklark Metasediments p282 Fig.13. See also Skylark Metamorphics.|1755+/-10 Ma zircon U-Pb, 1751+/-6 Ma zircon|Mount Woods Complex||Unconformably underlies Coodnambana Metaconglomerate. Intruded by Engenina Adamellite. Faulted against Balta Granite.|Migmatic paragneiss, orthogneiss and iron formations, includes felsic granulite gneiss, psammitic and pelitic gneisses. Poly-folded and polydeformed, overprinted by shear zones and leucocratic veins in parts.|05-SEP-22
73491|Skylark Metasediments|73235|6|Mentioned|p53, p58|Statherian|Orosirian|Gawler Craton. Mount Woods region. Hosts Prominent Hill and Cairn Hill IOCG mineralisation and Flintoft and Penrhyn orogenic gold mineralisation in the Mount Woods mineral field of the Kimban gold mineral system.|>1750 Ma|||||
27899|Sleaford Complex|22489|5|Briefly described|p12|Paleoproterozoic|Archean|||||||07-NOV-08
27899|Sleaford Complex|22494|5|Briefly described|p34|Archean|Archean|||||||07-NOV-08
27899|Sleaford Complex|22629|4|Described|p145, fig2p147|Archean|Archean|||||||07-NOV-08
27899|Sleaford Complex|22690|6|Mentioned|P305||Archean|||||||07-NOV-08
27899|Sleaford Complex|22834|6|Mentioned|P39||Archean|||||||07-NOV-08
27899|Sleaford Complex|23285|4|Described|p 335|||||||||
27899|Sleaford Complex|23481|5|Briefly described|p19 Fig 1|||Geological Province: Gawler Craton.||||||
27899|Sleaford Complex|23491|6|Mentioned|p17|Proterozoic|Archean|Includes the Carnot Gneisses.||||||07-NOV-08
27899|Sleaford Complex|23719|5|Briefly described|p12|Paleoproterozoic|Archean|See also page 14 table 1. Geological Province: Gawler Craton.||||||07-NOV-08
27899|Sleaford Complex|23791|5|Briefly described|p2|Archean|Archean|Geological Province: Gawler Craton.||||||07-NOV-08
27899|Sleaford Complex|23803|5|Briefly described|p28|Archean|Archean|Geological Province: Gawler Craton.||||||07-NOV-08
27899|Sleaford Complex|23805|5|Briefly described|p4 Fig. 1|Archean|Archean|Geological Province: Gawler Craton.||||||07-NOV-08
27899|Sleaford Complex|24261|5|Briefly described|p1047 Fig.1|Archean|Archean|Geological Province: Gawler Craton.||||||07-NOV-08
27899|Sleaford Complex|24296|5|Briefly described|p1250|Archean|Archean|Geological Province: Gawler Craton.||||||07-NOV-08
27899|Sleaford Complex|24365|5|Briefly described|p4, p5 Fig.2|Archean|Archean|Felsic paragneiss, mafic granulite and rare carbonate and magnetite-rich units.||||||07-NOV-08
27899|Sleaford Complex|24422|6|Mentioned|p84 Fig. 1|Archean|Archean|Geological Province: Gawler Craton.||||||07-NOV-08
27899|Sleaford Complex|24508|5|Briefly described|p30|Archean|Archean|Consists of Archaean para- and orthogneisses, granite, granodiorite, felsic and possible mafic volcanics, phyllite, tremolite marble and magnetite-rich metapelite.  Geological Province: Gawler Craton.||||||07-NOV-08
27899|Sleaford Complex|24522|6|Mentioned|p82|Archean|Archean|||||||07-NOV-08
27899|Sleaford Complex|24526|5|Briefly described|p95, p98|Paleoproterozoic||Consists of two components: Carnot Gneiss and Dutton Suite.  Geological Province: Gawler Craton.||||||07-NOV-08
27899|Sleaford Complex|24597|5|Briefly described|p526 Fig. 1|Archean|Archean|Age: ca2640-2300Ma.  Geological Province: Gawler Craton.  See also p525.||||||07-NOV-08
27899|Sleaford Complex|37461|6|Mentioned|Fig.5.2|||||||||
27899|Sleaford Complex|37620|6|Mentioned|p7|||||||||
27899|Sleaford Complex|37811|6|Mentioned|p222|||||||||
27899|Sleaford Complex|39345|6|Mentioned|Map legend|Paleoproterozoic|Archean|Archaean - Early Proterozoic||||||07-NOV-08
27899|Sleaford Complex|39349|6|Mentioned|Map legend|Paleoproterozoic|Archean|Archaean to Early Proterozoic||||||07-NOV-08
27899|Sleaford Complex|39352|6|Mentioned|Map legend|Proterozoic|Archean|||||||07-NOV-08
27899|Sleaford Complex|39353|6|Mentioned|Map legend|Paleoproterozoic|Archean|Archaean to Early Proterozoic||||||07-NOV-08
27899|Sleaford Complex|39762|6|Mentioned|Table 1|||||||||
27899|Sleaford Complex|39802|6|Mentioned|Map legend|Paleoproterozoic|Archean|||||||07-NOV-08
27899|Sleaford Complex|39844|6|Mentioned|p62|||||||||
27899|Sleaford Complex|40227|6|Mentioned|p44|||||||||
27899|Sleaford Complex|40448|4|Described|Table 2|||||||||
27899|Sleaford Complex|40644|4|Described|p120, p124 Fig. 3|Paleoproterozoic|Archean|Includes Sleaford Gneisses + Dutton Series (Tilley 1920, 1921), parts of Flinders Gp (Johns 1961), part of Flinders Gneiss (Whitten 1966), Carnot Gneisses (Fanning et al 1981) + Wangary Gneisses and Dutton suite (Fanning in Parker et al (1981) +Mitalie Gn||||||07-NOV-08
27899|Sleaford Complex|40942|6|Mentioned|p8|||||||||
27899|Sleaford Complex|41125|6|Mentioned|p30|||||||||
27899|Sleaford Complex|41239|5|Briefly described|p94|||||||||
27899|Sleaford Complex|41325|6|Mentioned|Fig.2|||||||||
27899|Sleaford Complex|41327|6|Mentioned|Fig.2|||||||||
27899|Sleaford Complex|41402|4|Described|p35|||Mention p41.||||||02-JUN-09
27899|Sleaford Complex|41493|6|Mentioned|Table 1|||||||||
27899|Sleaford Complex|41609|6|Mentioned|Fig. 1|||||||||
27899|Sleaford Complex|41619|6|Mentioned|Map legend|Tertiary||||||||
27899|Sleaford Complex|41667|5|Briefly described|p2|||||||||
27899|Sleaford Complex|41972|6|Mentioned|p365|||||||||
27899|Sleaford Complex|41973|6|Mentioned|Fig.1 P388|||||||||
27899|Sleaford Complex|42357|5|Briefly described|p8|||||||||
27899|Sleaford Complex|42466|5|Briefly described|Map Legend|||||||||
27899|Sleaford Complex|42468|5|Briefly described|p13, p14|||||||||
27899|Sleaford Complex|42475|5|Briefly described|p10|||||||||
27899|Sleaford Complex|42546|5|Briefly described|Map legend|Paleoproterozoic|Archean|||||||07-NOV-08
27899|Sleaford Complex|42716|5|Briefly described|Map legend|Archean||||||||07-NOV-08
27899|Sleaford Complex|42736|5|Briefly described|map legend|Paleoproterozoic||||||||07-NOV-08
27899|Sleaford Complex|42738|5|Briefly described|map legend|Archean||||||||07-NOV-08
27899|Sleaford Complex|42934|5|Briefly described|p520|||||||||
27899|Sleaford Complex|43049|5|Briefly described|p12|||||||||
27899|Sleaford Complex|43052|4|Described|p33|||Sedimentation greater than 2640 Ma.||||||21-OCT-08
27899|Sleaford Complex|43053|5|Briefly described|Map Legend|Paleoproterozoic|Archean|Metasedimentary and granitic gneiss, amphibolite (including pillow basalt, pyroxenite, komatiite); granitoids. Geological Province: southern Gawler Craton.||||||07-NOV-08
27899|Sleaford Complex|43141|6|Mentioned|p63,Fig.1||Archean|||||||07-NOV-08
27899|Sleaford Complex|43258|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
27899|Sleaford Complex|43298|5|Briefly described|Map Legend|Paleoproterozoic|Archean|||||||07-NOV-08
27899|Sleaford Complex|43561|6|Mentioned|p1434|||||||||
27899|Sleaford Complex|43595|5|Briefly described|p230|||||||||
27899|Sleaford Complex|50130|5|Briefly described|p2|Archean|Archean|Age: 3150 - 2950 Ma (U-Pb). Geological Province: Gawler Craton.||||||07-NOV-08
27899|Sleaford Complex|50605|5|Briefly described|p2.1, 8.7|Archean|Archean|Geological Province: Gawler Craton & Curnamona Province. Intruded by: Miltalie Gneiss, Donington Granitoid Suite, Minbrie Gneiss.||||||07-NOV-08
27899|Sleaford Complex|60484|5|Briefly described|p33 Fig. 1||| Geological Province: Gawler Craton.||||||
27899|Sleaford Complex|60515|6|Mentioned|p116 Fig.1 |||||||||
27899|Sleaford Complex|60534|5|Briefly described|p571, 572 Fig.1, 573 Fig.2|Archean|Archean|Metapelites. Geological Province: Gawler Craton. Age:>2600 Ma.||||||07-NOV-08
27899|Sleaford Complex|60704|5|Briefly described|p686 Fig.1|Archean|Archean|Geological Province: Gawler Craton||||||07-NOV-08
27899|Sleaford Complex|60707|5|Briefly described|p611|Archean|Archean|Geological Province: Gawler Craton (Coulter Domain).||||||07-NOV-08
27899|Sleaford Complex|60953|5|Briefly described|Map Legend|Archean|Archean|Age: 1440-1400 Ma (Metamorphic age).||||||07-NOV-08
27899|Sleaford Complex|60954|5|Briefly described|Map Legend|Archean|Archean|Geological Province: Gawler Craton.||||||07-NOV-08
27899|Sleaford Complex|61070|5|Briefly described|Map Legend|Proterozoic|Archean|Undifferentiated Archaean to earliest Proterozoic granitoids and gneisses. Geological Province: Gawler Craton.||||||08-JUL-13
27899|Sleaford Complex|61108|5|Briefly described|map legend|Archean|Archean|Paragneiss, granitic orthogneiss, iron formation and mafic granulite, granulite to amphibolite facies. Age: >2440-2400 Ma (metamorphic age).||||||07-NOV-08
27899|Sleaford Complex|61307|5|Briefly described|p35, p36 Fig. 17|Archean|Archean|Oldest crystalline basement sequence in the Gawler Craton. Includes: Carnot Gneisses, Dutton Suite intrusives, and Wangary Gneiss. See also p36 Fig. 17.||||||08-JUL-13
27899|Sleaford Complex|61393|6|Mentioned|p165, p169. |Paleoproterozoic|Archean|Metasediments. Separated from the Donington Suite granites by the Kalinjala Shear Zone.||||||
27899|Sleaford Complex|61522|5|Briefly described|p5 Fig.1|||Geological Province: Gawler Craton.||||||
27899|Sleaford Complex|61659|6|Mentioned|p30 Fig.1. |Archean|Archean|||||||
27899|Sleaford Complex|61725|5|Briefly described|p887|Archean|Archean|Overlain by the Hutchison Group metasediments.||||||07-NOV-08
27899|Sleaford Complex|61864|6|Mentioned|p16 fig 3|||||||||
27899|Sleaford Complex|62641|6|Mentioned|p277 Fig.1. |||||||||
27899|Sleaford Complex|62893|4|Described|Map Legend, p8, p26, p28|Early Proterozoic|Late Archean|Commonly migmatic and complexly folded; interleavered with the Hutchison Group. Associated with the Sleafordian Orogeny (2500-2300 Ma); at this time is was deformed at upper amphibolite to granulite facies metamorphism. Previously dated using Rb-Sr yielding ages of 2520 +/- 163 Ma and 2428 +/- 94 Ma.|||||Medium-grained and homogenous gneissic granodiorite, migmatitic and granitic gneiss with pegmatite and aplite veins, garnetiferous and migmatitic paragneiss, banded mafic granulite and iron formation.|
27899|Sleaford Complex|62898|6|Mentioned|p198|Paleoproterozoic|Archean|Age: 2700-2300Ma.||||||07-NOV-08
27899|Sleaford Complex|62978|5|Briefly described|p161|||Interlayered granulite-facies para- and orthogneisses. Geological Province: Gawler Craton.||||||07-FEB-11
27899|Sleaford Complex|63020|5|Briefly described|p971|Archean|Archean|Geological Province: Gawler Craton.||||||07-NOV-08
27899|Sleaford Complex|63223|5|Briefly described|p16, p17 Fig. 1, p19|Archean|Archean|Age: 2560-2500Ma. Metasedimentary and volcanic sequences. Geological Province: Gawler Craton.||||||07-NOV-08
27899|Sleaford Complex|63224|6|Mentioned|p10|||Metasediments and metavolcanics. Geological Province: Gawler Craton.||||||07-FEB-08
27899|Sleaford Complex|63275|5|Briefly described|p13, p14 Fig.1, p18, p20.|Archean|Archean|Oldest parts of Gawler Craton. Metamorphosed by early Paleoproterozoic Sleafordian Orogeny.||||||
27899|Sleaford Complex|63866|5|Briefly described|p3-p4|||||||Equivalent to the Mulgathing Complex.||
27899|Sleaford Complex|64130|6|Mentioned|p1378 Fig.1, p1380 Fig.2, p1382|Paleoproterozoic|Archean|See also p1836 Fig.5. Southern Gawler Craton.|~2550-2440 Ma|||||
27899|Sleaford Complex|64131|5|Briefly described|p1401, p1409 |Archean|Archean|Petrophysical properties.|2900? to 2430 Ma||Includes the Carnot Gneiss, Wangary Gneiss and Dutton Suite.|Correlated with the Mulgathing Complex.|Composed of banded iron formations (BIF), paragneiss and orthogneiss, amphibolite facies paragneiss, and weakly deformed granites.|
27899|Sleaford Complex|64137|5|Briefly described|p1542 Fig.1  |Archean|Archean|||||||
27899|Sleaford Complex|64313|5|Briefly described|p451 Figs.a,b|Archean|Archean|Geological province: Gawler Craton.||||||09-FEB-10
27899|Sleaford Complex|64573|5|Briefly described|p779, p780 Fig. 1|Mesoproterozoic|Neoarchean|Geological Province: Gawler Craton. Contains metamorphosed felsic to intermediate volcanic and sedimentary rocks emplaced or deposited between 25600 and 2500Ma.||||||07-FEB-11
27899|Sleaford Complex|64722|5|Briefly described|Fig. 2 p3-6, p12, 24, 27|Neoarchean||Southeast Gawler Province. Minimum age from 2480 Ma metamorphic zircon.||||Overlain by Hutchison Group.|Banded iron formation, carbonate, calc-silicate, quartzite and aluminous sedimentary rocks.|11-APR-12
27899|Sleaford Complex|64739|6|Mentioned|p264 Fig.1, p266, p280.|Archean|Archean|Gawler Craton.||||||
27899|Sleaford Complex|64740|6|Mentioned|p284 Fig.1. |Archean|Archean|||||||
27899|Sleaford Complex|64741|5|Briefly described|p299 Fig. 2|Archean|Archean|Age: 2550-2500Ma.||||||07-FEB-11
27899|Sleaford Complex|64828|5|Briefly described|p1064 Fig. 1|Paleoproterozoic|Late Archean|Comprises the Dutton Suite units (Whidbey and Kiana Granites, Coulta Granodiorite), Hall Bay Volcanics, Wangary Gneiss and Carnot Gneisses. Unconformably overlain by the Hutchison Group and Donington Suite granitoids. Geological province: Gawler Craton.||||||
27899|Sleaford Complex|65221|5|Briefly described|p26|Palaeoproterozoic|Neoarchaean|N-S trending metamorphosed metasedimentary and meta-igneous material. Intruded by ~2000 Ma felsic precursor to the Miltalie Gneiss||||||
27899|Sleaford Complex|65375|6|Mentioned|p13, p44.|Paleoproterozoic|Paleoproterozoic|Cleve and Spencer Domains, Gawler Craton. Also said to be Archean in text.||||||
27899|Sleaford Complex|65376|4|Described|p8 Fig.1.1, p15, p190. |Paleoproterozoic|Archean|Southern Gawler Craton. High-grade metamorphism and complex deformation from 1730-1700 Ma Kimban Orogeny. Shares many similarities with Mulgathing Complex; they may have been one continuous belt.|||Includes Carnot Gneiss and Dutton Suite.||Metasedimentary and felsic and mafic gneiss to granulite, including iron-formation.|
27899|Sleaford Complex|65385|6|Mentioned|pS131 Tab.2|||||||||
27899|Sleaford Complex|65390|6|Mentioned|p19, p23 Fig.3, p24|Siderian|Archean|Of Coulta Domain, Gawler Craton. Metasediments and volcanics. Age >2440 Ma. Sheared against Dutton Suite.||||||
27899|Sleaford Complex|65483|6|Mentioned|p17 Fig. 1|Archean|Archean|||||||
27899|Sleaford Complex|65485|5|Briefly described|p41-42, Fig 1|Archean|Archean|Southern Gawler Craton. Contains complexly deformed and metamorphosed units including the Carnot Gneisses, Wangary Gneiss, Hall Bay Volcanics, Dutton Suite. Timing of deformation discussed.||||||19-MAR-12
27899|Sleaford Complex|65772|6|Mentioned|p229 Fig.2|Paleoproterozoic|Archean|||||||
27899|Sleaford Complex|65915|5|Briefly described|p1-2, p3 Fig.2, p18|Siderian|Siderian|Gawler Craton basement. Protoliths to these gneisses include late Archean sediments and intercalated volcanics aged ~2550 -2500 Ma. Metamorphosed during Sleaford Orogeny (~2500-2400 Ma). Includes Carnot Gneiss. Overlain by Miltalie Gneiss and Hutchison Group. Gneisses. ~2450 Ma. Bounded on the east by Kalinjala Mylonite Zone.||||||
27899|Sleaford Complex|65922|5|Briefly described|p9, p12, p14 Tb. 1, p17 Tb. 2, p29 Fig.6|Paleoproterozoic|Neoarchean|Gawler Craton. Foliated migmatitic quartz-feldspar-biotite (garnet) gneiss and augen gneiss; possible local BIF. Interpreted to underlie Hutchison Group. Intruded by Gawler Range Volcanics. Garnet gneiss probably equivalent to Carnot Gneiss. Age inferred to be ~2600-2500 Ma.||||||20-MAR-15
27899|Sleaford Complex|66302|5|Briefly described|p4 Fig.3, p6, p10, p11, p13|Paleoproterozoic|Neoarchean|Coulta  and Cleve Domains, Gawler Craton. See also p14, p24, p26, p34, p56. |||Includes the Carnot Gneisses, Wangary Gneiss, Minbrie Gneiss, Hall Bay Volcanics and the Dutton Suite.|Intruded by the Hiltaba Suite. Equivalent to the Christie Gneiss. Overlain by the Hutchison Group.|Metasedimentary and volcanic rocks.|
27899|Sleaford Complex|66882|5|Briefly described|p101 Fig.1, p102 Fig.2, p116, p118, p120|Siderian|Neoarchean|Possible source rocks for c.2500 Ma zircons in Cleve Group.|2540-2450 Ma|||Unconformably underlies Warrow Quartzite.||
27899|Sleaford Complex|67058|5|Briefly described|p476, p490, p491, p492.|Neoarchean|Neoarchean|Southern Gawler Craton.|||Includes Carnot Gneiss, Wangary Paragneiss, Hall Bay Volcanics and Dutton Suite.|||
27899|Sleaford Complex|67181|6|Mentioned|p616 Fig.1|Archean|Archean|Gawler Craton. References: Fairclough et al. 2003, Payne et al. 2003.||||||
27899|Sleaford Complex|67536|5|Briefly described|Map Legend|||Gawler Craton. Inheritance to 3150 Ma.|||Includes Wangary Gneiss.||Paragneiss, granitic orthogneiss, iron formation, mafic granulite.|
27899|Sleaford Complex|67721|6|Mentioned|p35 Fig.5|||||||||
27899|Sleaford Complex|67980|6|Mentioned|p550|Proterozoic|Archean|Coulta Domain, southern Gawler Craton. Deformed and metamorphosed during Sleafordian Orogeny, between ca 2470 and 2410 Ma.||||||
27899|Sleaford Complex|68128|5|Briefly described|p1-p2, p5-7|Palaeoproterozoic|Archaean|Gawler Craton. Deformed, metamorphosed and intruded by syn-tectonic felsic and mafic intrusions during the 2460-2420 Sleafordian Orogeny. Prospective for a range of commodities including gold, nickel, copper, PGE and iron ore.|ca 2555-2510 Ma||Includes the Hall Bay Volcanics and the Kiana Granite.||Komatiites, basalts, acid volcanics and interbedded iron formation, carbonates and carbonaceous clastics.|
27899|Sleaford Complex|68131|5|Briefly described|p2 Fig.1, p84|Paleoproterozoic|Archean|Associated with Sleafordian Orogeny. Mapped with Mulgathing Complex as a single unit.|||||Metasedimentary and felsic and mafic gneiss to granulite, including iron formation.|
27899|Sleaford Complex|68208|5|Briefly described|p31, p35, p37 Fig.10, p39|Paleoproterozoic|Neoarchean|Affected by the 2470 - 2420 Ma Sleafordian Orogeny.|2555 - 2450 Ma||Includes Coulta Granodiorite, Hall Bay Volcanics, Wangary Gneiss, Carnot Gneiss||Volcanosedimentary and plutonic rock association.|
27899|Sleaford Complex|69004|6|Mentioned|p18|||Gawler Craton.||||||
27899|Sleaford Complex|69048|4|Described|p2-3, p18, p37-53|||Southern Eyre Peninsula. Separated from the Donington Suite to the east by the Kalinjala Shear Zone. Youngest sedimentary protolith ages recorded are c.2515 Ma (Swain et al., 2005). SHRIMP U-Pb zircon ages of magmatic crystallisation of igneous protoliths. The 2506 Ma age is of a granoblastic two-pyroxene gneiss, metamorphosed at 1731 +/- 7 Ma. The 2421 Ma age is of a garnetiferous gneiss the igneous protolith of which intruded, and was later folded into, the metasedimentary sequence; high-grade metamorphism occurred at 1731 +/- 5 Ma (Kimban Orogeny).|2506 +/- 6 Ma; 2421 +/- 7 Ma.|||Correlative of Mulgathing Complex.|Includes a garnet-bearing quartzofeldspathic gneiss and a mafic two-pyroxene gneiss.|
27899|Sleaford Complex|69203|6|Mentioned|p35|||Southern Gawler Craton.|||Hall Bay Volcanics.|||
27899|Sleaford Complex|69213|5|Briefly described|p30-31, 24|Paleoproterozoic|Neoarchean|Gawler Craton. Metamorphosed in Sleafordian Orogeny. Remetamorphosed in Kimban Orogeny ~1700 Ma. Similar in composition and age to the Mulgathing Complex. Includes granitic gneiss with emplacement age of 2431 +/-7 Ma and metamorphic zircon growth at 1715+/- 6 Ma (SHRIMP dating). Also undeformed  S-type granite 2414 +/-6 Ma.||||Considered lateral equivalent of Mulgathing Complex.|Migmatites and garnet-cordierite bearing megacrystic granitic gneiss and metapelitic gneiss. Schollen diatexites and layered diatexite, garnet-cordierite S type granites that are locally intruded by hornblende bearing mafic dykes.|
27899|Sleaford Complex|69554|6|Mentioned|p128, 130, 136|Paleoproterozoic|Paleoproterozoic|Southern Gawler Craton. Forms basement, which is inferred to be at least in part derived from Mesoarchean crust.|c.2530-2410 Ma.|||||
27899|Sleaford Complex|69595|5|Briefly described|p37|Neoarchean|Neoarchean|Gawler Craton. Interpreted to have formed by interaction of a convergent margin and mantle plume with the sedimentary component having deposited in a back-arc or arc-rift basin setting.|c. 2560-2500 Ma||||Metasedimentary rocks and generally coeval felsic and mafic to ultramafic volcanic rocks.|
27899|Sleaford Complex|69649|6|Mentioned|p6 Fig.4,|||||||||
27899|Sleaford Complex|70023|6|Mentioned|p182|||Geological province: Gawler Craton.||||||
27899|Sleaford Complex|70027|4|Described|p55-58,71,72|Paleoproterozoic|Neoarchean|Geological province: Gawler Craton. Sedimentary and volcanic units deposited during 2560-2480 Ma. Deformed and underwent LPHT metamorphism during the 2465-2420 Ma Sleaford Orogeny (Fanning 1997; Swain et al. 2005; Jagodzinski et al. 2012; Reid et al. 2014). Intruded by magmatic rocks during 1730-1690 Ma Kimban Orogeny. Contains ca. 2875 Ma detrital zircons, sources unknown. Also contains ca 2530-2500 Ma zircons, derived from various locally sourced igneous intrusions. Magnetite-poor lithologies at Warramboo are likely part of Sleaford Complex basement (Daly and Fanning 1993; this study) and are much older than magnetite-rich lithologies of the Warramboo magnetite gneiss.|||Includes Dutton Suite.|||
27899|Sleaford Complex|70286|6|Mentioned|p884|||Eastern Gawler Craton.||||||
27899|Sleaford Complex|70334|5|Briefly described|p74|Paleoproterozoic|Neoarchean|Geological province: Gawler Craton. ||||Equivalent to Cooyerdoo Granite.||
27899|Sleaford Complex|70511|6|Mentioned|p87, 96|Archean|Archean|Gawler Craton.|2500 Ma.|||||
27899|Sleaford Complex|70721|6|Mentioned|p63, p73|Neoarchean|Neoarchean|Spencer Domain, Gawler Craton. Basement of the Spencer Domain.|2550-2440 Ma|||||
27899|Sleaford Complex|70893|6|Mentioned|p3 fig 1a||||c.2530 - 2410 Ma|||||05-SEP-19
27899|Sleaford Complex|70947|6|Mentioned|p960|Paleoproterozoic|Archean|Geological province: Gawler Craton.|ca. 2530-2410 Ma|||||
27899|Sleaford Complex|71037|5|Briefly described|p21 Fig.1|Archean|Archean|Shown only on 'Outcropping geology and mineral deposits of northern Eyre Peninsula' map p21 Fig.1. These Archean rocks are shown in the southeastern part of the Eyre Peninsular.||||Shown as younger than Coolanie Gneiss and Cooyerdoo Granite.|Metamorphically evolved and reworked metapelites.|
27899|Sleaford Complex|71043|5|Briefly described|p104, p107, p115|Paleoproterozoic|Neoarchean|Southern Gawler Craton.|c.2530-2410 Ma.||Hall Bay Volcanics.|||
27899|Sleaford Complex|71129|5|Briefly described|p14,17-18,23,41,203|Neoarchean|Neoarchean|Geological Province: Cleve-Coulta and Spencer domains, Gawler Craton. Sediments and felsic volcanics deformed and intruded by felsic to intermediate magmas during Sleafordian Orogeny (2465-2410 Ma).||||Overlies the Coolanie Gneiss.||13-NOV-19
27899|Sleaford Complex|71235|6|Mentioned|p14|||||||||
27899|Sleaford Complex|71236|5|Briefly described|p2|Archean|Archean|||||||
27899|Sleaford Complex|71317|5|Briefly described|p14, p16|||Cleve-Coulta Domains, Gawler Craton.||||||
27899|Sleaford Complex|71322|5|Briefly described|p3, p91, p135|Paleoproterozoic|Neoarchean|Forms basement to the Cleve Domain. Deformed at 1718 +/- 6 M, during the Kimban Orogeny. Hosts the Telephone Dam prospect, and the Mawson Cu-Fe prospect hosted by a leucogranite dated 2473 +/- 8 Ma.|c.2560-2440 Ma.|||Is overlain by the Cleve Group.|Includes leucogranite gneiss.|
27899|Sleaford Complex|71341|6|Mentioned|p179 fig 1, p198|Palaeoproterozoic|Neoarchean||ca. 2530-2410 Ma|||||
27899|Sleaford Complex|71348|6|Mentioned|p201|Paleoproterozoic|Archean|Geological province: Gawler Craton.||||||
27899|Sleaford Complex|71418|6|Mentioned|p21|Paleoproterozoic|Archean|Geological province: Gawler Craton.||||||
27899|Sleaford Complex|71534|6|Mentioned|p295-p296|Paleoproterozoic|Neoarchean|Geological province: Gawler Craton.||||||
27899|Sleaford Complex|71559|6|Mentioned|p15 Fig 1, p16 Fig 2|Archean|Archean|Geological province: Gawler Craton. Also referred to as Sleaford-Mulgathing Complexes.||||||
27899|Sleaford Complex|71859|4|Described|p1-p4, p6-p8, p10-p12, p14|Archean|Archean|Southern Gawler Craton, Cleve, Coulta and Spencer domains. First introduced by Thomson (1980) to describe late Archaean to early Paleoproterozoic granites, orthogneisses and paragneisses on Eyre Peninsula. Recent geochronology [this volume] reassigned the Minbrie Gneiss and the Carpa Granite to this complex. Forms basement in the southern Gawler Craton and occurs extensively along the entire length of the western Eyre peninsula. Lithologically similar to Mulgathing Complex in the northern Gawler Craton. Comprises two phases: an older phase of sedimentary units, felsic and mafic volcanics and intrusives ranging from 2600-2470 Ma and a younger phase of intrusives emplaced during the Sleafordian Orogeny (2470-1410 Ma). Underwent metamorphism during the Sleafordian Orogeny and the Kimban Orogeny. See also  p17-p18, p20, p24-p29, p35-p36.|2600-2410 Ma||Includes the Hall Bay Volcanics, Wangary Gneiss, Carnot Gneiss, Dutton Suite, Minbrie Gneiss and the Carpa Granite.|Intruded by the Lincoln Complex and Peter Pan Supersuite. Overlies the Cooyerdoo Granite and the Coolanie Gneiss. Overlain by the Hutchison Group.|A range of lithologies from pelitic metasedimentary rocks, felsic to komatiitic volcanics and A- and S-type granites.|06-APR-23
27899|Sleaford Complex|71862|5|Briefly described|p1-p5, p7-p8, p12|Siderian|Neoarchean|Forms basement to the southern Gawler Craton, originally interpreted to be intruded by the now obsolete Lincoln Complex. Geochemical relationship with the Moola and Pinbong Suites are discussed. See also p15-p16, p44, p52, p54, p58.|c. 2565-2410 Ma|||Intruded by the Burkitt Granite. Faulted against the Donington Suite.||
27899|Sleaford Complex|72058|5|Briefly described|p172, 192|Neoarchean|Neoarchean|Forms basement of the Spencer Domain, Gawler Craton. Deformed during the 2.47-2.41 Sleafordian Orogeny.|2540-2450 Ma|||Overlain by the Middleback Group.||16-MAR-21
27899|Sleaford Complex|72090|4|Described|p10, p11, p14, p60-p65, p73|Paleoproterozoic|Archean|Cleve-Coulta Domain, Gawler Craton. Can be distinguished from GRV volcanics based on differences in geochemistry. Additional sample lithologies are described. See also p78, p80-p81, p98, p102, p111.|2550-2440 Ma|||Unconformably overlain by the Waganny Dacite.|Greyish pink to greenish grey, fine- to very coarse-grained, variably pegmatitic, feldspar-quartz-sericite-biotite-chlorite orthogneiss, metagranite and amphibolite.|
27899|Sleaford Complex|72462|6|Mentioned|p3, p10|Siderian|Neoarchean|Gawler Craton.|2550-2440 Ma|||Overlain by Hutchison Group.|Orthogneiss.|
27899|Sleaford Complex|72463|6|Mentioned|p2|Archean|Archean|||||||
27899|Sleaford Complex|72464|6|Mentioned|p2|Paleoproterozoic|Archean|Gawler Craton.||||||
27899|Sleaford Complex|72484|5|Briefly described|p2|||Gneissic basement formed by amphibolite- to granulite-facies metamorphism of the Sleafordian Orogeny.|~2.47-2.41 Ga.|||||
27899|Sleaford Complex|72949|6|Mentioned|p34|Siderian|Neoarchean||ca. 2.53-2.41 Ga|||||
27899|Sleaford Complex|73026|5|Briefly described|p4 fig1.2, p5-6, p14|early Paleoproterozoic|Neoarchean|Occurs on the central/western Eyre Peninsula. The oldest component of this complex was protolith to the Coolanie Gneiss. See also p9, p25.|c. 2560-2440 Ma|||Underlies the Gawler Range Volcanics.|Metasediment, metabasalt, sills, dykes; augen gneiss. Granulite to amphibolite facies metamorphism.|
27899|Sleaford Complex|73027|5|Briefly described|p4, p9-10, p14-15|Palaeoproterozoic|Neoarchaean|Deformed by the Sleafordian orogeny at c. 2465-2410 Ma. See also p40-41.|>2400 Ma (protoliths)||||Metasediment, metabasalt, sills, dykes, augen gneiss, granulite to amphibolite facies metamorphism.|
27899|Sleaford Complex|73030|6|Mentioned|p2148-2149|Siderian|Neoarchean|Gawler Craton.|ca. 2530 - 2410 Ma|||||
27899|Sleaford Complex|73104|4|Described|p1-5, p11, p19, p41, p46-47, p51-76|Neoarchean|Neoarchean|Geochron includes magmatic crystallisation ages of 2481 +/- 13 Ma, 2487 +/- 130 Ma, 2483 +/- 5 Ma, c. 2470 Ma. Contains older inherited zircons going back in age to about 3000 Ma (2522 +/- 14 Ma), indicating the presence of an underlying Mesoarchean basement. Records metamorphism relating to the Sleaford Orogeny (2425 +/- 10 Ma) and Kimban Orogeny (1716 +/- 7 Ma, 1723 +/- 8 Ma). Part of the unexposed portion consists of volcano-sedimentary rocks that are probably correlatives of the Hall Bay Volcanics. Inferred basement rock of the Mount Double area. [Article includes petrographic description].|2470-2480 Ma||Dutton Suite|Equivalent to Kiana Granite. Overlain by Waganny Dacite. Intruded by Peter Pan Supersuite.|Foliated and metamorphosed peraluminous two-mica granites (augen-orthogneisses). Includes medium- to coarse-grained, granoblastic, leucocratic orthogneiss, and reddish-brown, variably deformed, coarse-grained, feldspar-porphyritic orthogneiss.|
27899|Sleaford Complex|73110|5|Briefly described|Map legend.|Paleoproterozoic|Archean||||Minbrie Gneiss.||Metasediment; metabasalt, sills, dykes; augen gneiss. Granulite facies, amphibolite facies.|
27899|Sleaford Complex|73122|5|Briefly described|p18 Fig.1, p19, p21 Fig.4, p22, 29|Palaeoproterozoic|Archaean|Gawler Craton. See also p35, 40-41.|~2550-2410 Ma.||||Includes charnockites, garnet-sillimanite paragneisses, sheared quartz-feldspar gneisses.|
27899|Sleaford Complex|73130|6|Mentioned|[poster]|Siderian|Neoarchean|Constitutes basement beneath the Itiledoo Basin.|c. 2560-2470 Ma|||||
27899|Sleaford Complex|73155|6|Mentioned|p264 Fig.1|Siderian|Neoarchean|Gawler Craton.|ca. 2530-2410 Ma|||||
27899|Sleaford Complex|73162|6|Mentioned|p449, Fig.1|||||||||
27899|Sleaford Complex|73165|6|Mentioned|p621, p634-635|Paleoproterozoic|Neoarchean|Gawler Craton, southern. Formed from basin development, bimodal magmatism and sedimentation. Basin deveopment terminated in the Sleafordian Orogeny ca 2480-2420 Ma.||||||
27899|Sleaford Complex|73166|6|Mentioned|p644|Neoarchean|Neoarchean|Gawler Craton, eastern.|ca 2.5 Ga|||||
27899|Sleaford Complex|73230|6|Mentioned|p15||||||Kiana Granite, Dutton Suite|||
27899|Sleaford Complex|73233|6|Mentioned|p27 Fig.1|Paleoproterozoic|Archean|Gawler Craton.||||||
27899|Sleaford Complex|73234|6|Mentioned|p18|||Eyre Peninsula, western.|||||Volcano-sedimentary rocks.|
27899|Sleaford Complex|73235|6|Mentioned|p52-53, p55-58|Siderian|Neoarchean|Gawler Craton. Olympic, Spencer, Cleve, Coulta, and Gawler Range Volcanic regions. Hosts gold mineralisation in the Kyancutta mineral field of the Sleafordian gold mineral system. Hosts Hall Bay; WUD2C and Bramfield orogenic gold mineralisation. Occasionally thrust over the Hutchison Group.|c. 2555-2410 Ma|||||
27899|Sleaford Complex|73256|4|Described|p557-562, p564-568, p570-576|Siderian|Siderian|Gawler Craton. Extension/rift setting. Compressional deformation. Prospective for Au, Ni, Cu, PGEs, and Fe. [See article for petrographic descriptions, whole-rock geochemistry, and zircon morphological and compositional characterisation].|ca 2450 Ma||Carnot Gneisses, Wangary Gneiss, Hall Bay Volcanics, Dutton Suite||Includes medium- to high-grade metasedimentary successions.|
27899|Sleaford Complex|73298|6|Mentioned|p1072 Fig.1, p1073, p1078 Fig.6|Neoachean|Neoarchean|Gawler Craton, central-western. Nawa, Christie and Coulta domains. Represents volcano-sedimentary basins terminated during and deformed by the 2480-2420 Ma Sleafordian Orogeny.|ca 2506 Ma|||||
27899|Sleaford Complex|73302|6|Mentioned|p53|Neoarchean|Neoarchean|Despite being adjacent to, or within close proximity of, the St Peter Suite, there are no inherited Archaean zircons in the latter.||||||
27899|Sleaford Complex|73493|6|Mentioned|p714 Fig.1, p716 Fig.3|Siderian|Neoarchean|Gawler Craton.|c.2530-2410 Ma|||||
27899|Sleaford Complex|73634|6|Mentioned|p2 Fig.1, p4, 16-17|Archean|Archean|Drexel et al. (1993). This name is used for the elevated Gawler Craton nucleus in the southern Eyre Peninsula. Records both the Sleafordian (2000-1845 Ma) and Kimban (1730-1690 Ma) Orogenies.||||||
27899|Sleaford Complex|74361|6|Mentioned|p163|||Eastern Gawler Craton. Deformed by the Sleafordian (~2480-2420 Ma) and Kimban (~1730-1690 Ma) Orogenies.|~2500 Ma.|||||
82224|Sloan Hill Tonalite|73230|2|Defined|p6-7, p12, p14|Neoarchean|Neoarchean|New name [see appendix and ASUD for definition]. Gawler Craton. Domain: Eastern Mulgathing Complex. No known outcrop. Ar-Ar geochronology of sericite and K-feldspar suggest hydrothermal alteration occurred at c. 1.6 Ga; coeval with emplacement of the Hiltaba Suite and Gawler Range Volcanics. Named after Sloan Hill on the BILLA KALINA mapsheet. Previously known informally as 'hematite-stained tonalite' and 'Mulgathing Complex unit 8'. Type locality: drillhole (DDH) SH 7C (SA Geodata drillhole 237530), interval 1,427-1,467.5 m. Minimum thickness: 40.5 m (base not intersected in type drillhole). Age [also written as c. 2530 Ma] is zircon SHRIMP U-Pb from Jagodzinski and Reid (2017).|c. 2529 Ma (magmatic)|Mulgathing Complex||Unconformably overlain by Pandurra Formation.|Massive, hematite-stained granite-tonalite with zones of sericite-chlorite alteration.|
23976|Snapper Point Sand Member|22525|6|Mentioned|p37,39,40||Pleistocene|Part of the Ngaltinga Formation.|||||Clayey sand and clay with occasional sandy interbeds.|24-AUG-18
23976|Snapper Point Sand Member|41551|6|Mentioned|p465|||||||||
23976|Snapper Point Sand Member|70660|5|Briefly described|p9|||||Ngaltinga Formation||||
29819|South Lake Gabbro|24472|5|Briefly described|p5 Tb.1|Archean|Archean|Geological Province: Harris Greenstone Domain, Gawler Craton. Age: 2430 Ma (metazircon). Parent: Mulgathing Complex.||||||07-NOV-08
29819|South Lake Gabbro|43052|4|Described|p42, Table 3.2|||Of Mulgathing Complex||||||
29819|South Lake Gabbro|50605|5|Briefly described|p8.7|||Of the Mulgathering Complex. Geological Province: Gawler Craton & Curnamona Province.||||||
29819|South Lake Gabbro|65376|6|Mentioned|p190.|||||Unit in Mulgathing Complex.||||
29819|South Lake Gabbro|66302|6|Mentioned|p12, p13|||Metamorphic SHRIMP age of 2440 +/- 9 Ma (Fanning et al, 1997). ||Mulgathing Complex|||Gabbro.|
29819|South Lake Gabbro|68128|6|Mentioned|p2|Palaeoproterozoic|Archaean|Gawler Craton.||Mulgathing Complex||||
29819|South Lake Gabbro|73230|4|Described|p6, p8, p12|||Gawler Craton. Domain: Harris Greenstone. Metamorphism at c. 2440-2430 Ma. Interlayered with Kenella Gneiss. Consists of thin (1-2 m) sill-like metagabbro bodies. Intrusive age and emplacement style are not well constrained but may be an intrusive equivalent of Hopeful Hill Basalt (further work is needed).||Mulgathing Complex||Intruded [crosscut] by Glenloth Granite.|Plagioclase-rich metagabbro with hornblende, diopside and quartz.|
38066|Southern Right Supersequence|24336|5|Briefly described|p99 Fig.3|||Correlated to the Neptune Formation.||||||
38066|Southern Right Supersequence|61544|6|Mentioned|p367 Fig.3. |Berriasian|Berriasian|Ceduna Sub-basin. Post-rift slow thermal subsidence.||||Overlies Minke Supersequence. Is overlain by Bronze Whaler Supersequence.||
38066|Southern Right Supersequence|66578|6|Mentioned|p1007 Fig.3.|Early Cretaceous|Early Cretaceous|Ceduna Sub-Basin, Bight Basin.||||Overlies Minke Supersequence. Is overlain by Bronze Whaler Supersequence.||
38066|Southern Right Supersequence|69297|5|Briefly described|p14 fig 2.4, p23, p25 fig 2.9|Valanginian|Berriasian|Eyre, Ceduna and Duntroon Sub-basins. Deposited in lacustrine and fluvial environments. Basal sands of this sequence display high measured porosity and permeability and are thus good potential reservoirs for petroleum. Contains potential source rocks within lacustrine shales and coaly deposits. See also p26 fig 2.11, p27, p28, p37, p42, p45 fig 2.17, p58, p60, p61. ||||Overlies the Minke Supersequence. Overlain by the Bronze Whaler Supersequence.|Interbedded claystone, siltstone, snadstone and coal.|
38066|Southern Right Supersequence|70067|5|Briefly described|Ceduna: Fig.2. Regional: Fig.2|Valanginian|Berriasian|Bight Basin. Copmprises Neptune Formation and topmost Echidna Formation.||||Overlies Minke Supersequence. Is overlain by Bronze Whaler Supersequence.||
34731|Spalding Dolomite Member|22889|2|Defined|p33 & p37|Adelaidean|Adelaidean|Type section location advised p37.  The Spalding Dolomite Member thins to the south, see p38.||||||
79615|Spearfelt Rhyodacite|71037|5|Briefly described|p21, p27 Fig.6|Mesoproterozoic|Mesoproterozoic|The youngest unit of the lower Gawler Range Volcanics, in this area.||Gawler Range Volcanics (Lower)||Shown as younger than Roopena Basalt and older than Eucarro Rhyolite or Gawler Range Volcanics (Upper).|Rhyodacite, red-brown, porphyritic, phenocrysts of feldspar, pyroxene, hornblende and lesser quartz in a fine-grained groundmass.|
79615|Spearfelt Rhyodacite|71129|3|Fully described|p47,49,51,53,59,64,68,78|Calymmian|Calymmian|Geological Province: Gawler Craton. Also referred to as Spearfelt Rhyolite in text. Occurs in outcrop as a ~20x12km large, NE trending elongate body between Parkinson Dam and Six Mile Hill. Named for Spearfelt Dam located 6 km southwest of the Myall Creek Homestead.  Originally mapped as Nonning Rhyodacite in the Myall Creek area, but later renamed Eucarro Rhyolite. Thereafter CA-TIMS dating has shown that these rocks are significantly older than the Eucarro Rhyolite or Nonning Rhyodacite, these these units have been defined as the new Spearfelt Rhyodacite. Outcrops range from small rubbly rises to broad low hills and are bound to the NW and SE by NE-trending Uno and Trevor faults respectively. May extend in the subsurface further northeast beyond the Roopena Fault. Separated from Broadview Schist via Trevor Fault, and Eucarrop Rhyolite via Uno Fault. Thickness: 20-30m in outcrop, up to 97m as intersected in MSDP03. Depositional environment: subaerially extruded lava flow, based on coherent nature of lava flows and absence of volcaniclastic facies. Lithology is described in some detail.  U-Pb CA-TIMS age of 1591.2+\-0.5 Ma (Jagodzinski, pers. comm. 2016). See also p84-90, 98, 112,114,184,189-190,206-207,225,227.|1591.2+\-0.5 Ma (U-Pb CA-TIMS)|Unit of Gawler Range Volcanics.||Overlain by Tapley Hill Formation or Pandurra Formation. Underlain by Corruna Conglomerate or Broadview Schist or Roopena Basalt. Uppermost unit of lower GRV.|Reddish- to purplish-brown, massive, porphyritic feldspar phyric rhyolitic to dacitic volcanic rock with local xenoliths of aphyric flow-laminated rhyolite.|13-NOV-19
79615|Spearfelt Rhyodacite|71130|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|||Lower Gawler Range Volcanics.|||Red-brown porphyritic rhyodacite, with phenocrysts of feldspar, pyroxene, hornblende and lesser quartz in a fine-grained groundmass.|
79615|Spearfelt Rhyodacite|71131|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|||Lower Gawler Range Volcanics.|||Red-brown porphyritic rhyodacite, with phenocrysts of feldspar, pyroxene, hornblende and lesser quartz in a fine-grained groundmass.|
79615|Spearfelt Rhyodacite|71414|5|Briefly described|p42 Fig 1, p43|Mesoproterozoic|Mesoproterozoic|Geological province: Gawler Craton. Outcrops extensively in the Six Mile Hill area.||Unit of Gawler Range Volcanics.||Underlain by quartz-phyric rhyolitic ignimbrite near Junction Dam, mafic volcanics near Princefoot Dam, and a vitriclastic ash tuff at Nine Mile Dam (McAvaney etal., 2016).|Feldspar-phyric evenly porphyritic|
79615|Spearfelt Rhyodacite|72089|4|Described|p2-p3, p5, p7, p12|||Gawler Craton. Most of the Gawler Range Volcanics outcrop that occurs between Six Mile Hill and Spearfelt Dam is mapped as this unit. Overlies an unnamed rhyolitic ignimbrite. Rocks previously mapped as this unit are now reinterpreted as the informal 'Upper felsic volcanic unit' and a "Felsic volcanic unit' of the Gawler Range Volcanics.||Gawler Range Volcanics, lower|||Massive, feldspar-phyric, crystal-rich rock interpreted to be a coherent lava.|
79615|Spearfelt Rhyodacite|72090|5|Briefly described|p39-p40, p42, p44, p108|||Gawler Craton. Downhole magnetic susceptibilites were low. Average specific gravity measurements ar 2.61 g/cc.|||||Moderate reddish brown to very pale orange, phenocrystic, medium grained, fresh to highly weathered, very fractured rhyodacite.|
79615|Spearfelt Rhyodacite|73162|5|Briefly described|p451|Calymmian|Calymmian||1591.2 +/- 0.5 Ma|||Conformably overlies the Roopena Basalt.||
79320|Sprigg Diamictite Member|70383|2|Defined|p42-53|Valanginian|Berriasian|New name, after Sprigg Nob, 4km NW of Arkaroola Tourist Complex. The type section is the Sprigg costean near the E flank of Mount Gee (340845mE, 6655290mN). A subsidiary section is in CRAE drillcore DD91GE33. Distribution limited to a few kms to W and E of Mount Gee, Mount Painter Inlier. Not a bedded unit; forms steeply-dipping dyke-like bodies within chloritic brecciated granite, up to 2m wide and locally over 100m long. Interpreted as glacial till infill of a crevice. Has undergone chloritic alteration. Looks similar to the Merinjina Tillite c.9 km to the SSE. Sediment provenance and lithological interpretations discussed. Maximum depositional age radiometric age of detrital zircons. Stated likely depositional age presumably based on correlation with Livingston Tillite Member.|<264 +/- 3 Ma (LA-ICPMS).|Of Cadna-owie Formation.||Crosscuts Radium Ridge Breccias. Is crosscut by Mount Gee Sinter. Equivalent to Livingston Tillite Member.|Tillite. Clast- to matrix-supported. Clasts (felsic volcanics and quartzite) are well-rounded to sub-angular, mostly pebbles and cobbles (ranging from granules to boulders). Dark red-brown or grey-green, silty-sandy matrix.|23-JAN-19
79320|Sprigg Diamictite Member|70384|5|Briefly described|Map legend.|Early Cretaceous|Early Cretaceous|Maximum depositional age from detrital zircons.|<264 +/- 3 Ma (U-Pb detrital zircons).|Of Cadna-owie Formation.|||Fluvial-glacial sediment; crevice fill.|23-JAN-19
24502|St Peter Suite|22494|5|Briefly described|p34|||||||||
24502|St Peter Suite|22613|6|Mentioned|p11|||||||||
24502|St Peter Suite|22629|6|Mentioned|fig2p147|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
24502|St Peter Suite|23342|5|Briefly described|28 Fig.1|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
24502|St Peter Suite|23481|5|Briefly described|p19 Fig 1|||Geological Province: Gawler Craton.||||||
24502|St Peter Suite|23805|5|Briefly described|p4 Fig. 1|Paleoproterozoic|Paleoproterozoic|Geological Province: Gawler Craton.||||||04-JUN-09
24502|St Peter Suite|24197|6|Mentioned|p74 Tb. 8.1|Paleoproterozoic|Paleoproterozoic|Age: 1625Ma. Geological Province: Gawler and Curnamona Cratons.||||||07-FEB-11
24502|St Peter Suite|24422|6|Mentioned|p84 Fig. 1|Paleoproterozoic|Paleoproterozoic|Geological Province: Gawler Craton. See also St Peters Suite.||||||07-NOV-08
24502|St Peter Suite|24505|5|Briefly described|p5 Fig. 1, p6|||Geological Province: Gawler Craton.  Saint is St in text.||||||18-JAN-07
24502|St Peter Suite|24526|5|Briefly described|p100|||Granitic pluton.  Age: 1620Ma.  Geological Province: Gawler Craton.||||||04-JUN-09
24502|St Peter Suite|24597|5|Briefly described|p526 Fig. 1|Paleoproterozoic|Paleoproterozoic|Age: ca1620Ma.  Geological Province: Gawler Craton.  See also p528 Fig. 3, p526.||||||04-JUN-09
24502|St Peter Suite|42291|2|Defined|p2|Proterozoic|Paleoproterozoic|Age: 1620 +/-4Ma.||||||08-JAN-16
24502|St Peter Suite|42292|6|Mentioned|Fig.1 P9|||||||||
24502|St Peter Suite|42466|5|Briefly described|Map Legend|||||||||
24502|St Peter Suite|42470|6|Mentioned|p18|||||||||
24502|St Peter Suite|42475|4|Described|p11|||||||||
24502|St Peter Suite|43052|4|Described|p81|||Actually spelt St Peter Suite.||||||12-DEC-06
24502|St Peter Suite|60484|5|Briefly described|p33 Fig. 1|Statherian|Statherian|Tonalitic to granite suite.  Age: 1630-1608Ma.  Intruded into the Nuyts Domain.  Geological Province: Gawler Craton. See also p38.||||||04-JUN-09
24502|St Peter Suite|60496|5|Briefly described|p22 Fig. 1|Paleoproterozoic|Paleoproterozoic|||||||04-JUN-09
24502|St Peter Suite|60515|6|Mentioned|p116 Fig.1 |||||||||
24502|St Peter Suite|60707|5|Briefly described|p611|||Deformed and foliated granite and monzogranite contain local mylonite zones.  Occurs south of Ceduna - probably same suite as the Palaeoproterozoic St Peters Suite also mentioned?||||||12-DEC-06
24502|St Peter Suite|60953|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Age: 1620Ma. Comagmatic granitoids and mafic intrusives.||||||07-NOV-08
24502|St Peter Suite|60954|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Geological Province: Gawler Craton. Granitoids, volcanics and inferred basic dykes.||||||
24502|St Peter Suite|61108|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|Spelt St on map legend. Comagmatic granite to granodiorite and diorite, dolerite and amphibolite. Age: 1620 Ma.||||||07-NOV-08
24502|St Peter Suite|61262|5|Briefly described|p455 Fig. 11|Paleoproterozoic|Paleoproterozoic|Age: >1600Ma. Geological Province: western Gawler Craton. (St. is correct for Saint).||||||07-NOV-08
24502|St Peter Suite|61393|5|Briefly described|p164, p166 Fig.1, pp175-177.     |Paleoproterozoic|Paleoproterozoic|Central Gawler Craton. Regional, voluminous, syn-deformational, arc-like magmatism.|c.1630 - 1610 Ma.||||Tonalites to granodiorites.|
24502|St Peter Suite|61522|5|Briefly described|p5 Fig.1|||Geological Province: Gawler Craton.||||||04-JUN-09
24502|St Peter Suite|61659|6|Mentioned|p30 Fig.1. |Paleoproterozoic|Paleoproterozoic|||||||
24502|St Peter Suite|61864|5|Briefly described|p16 fig 3, p17|||Distinct circular aeromagnetic signature.|~1630 Ma (Flint et al. 1990).||||Granites to diorites.|
24502|St Peter Suite|62898|5|Briefly described|p200, p202 Fig. 4, p204|Paleoproterozoic|Paleoproterozoic|Of the Linclon Complex.  Age: 1620+/-4Ma (Flint et al, 1990).||||||07-NOV-08
24502|St Peter Suite|62978|5|Briefly described|p161|Mesoproterozoic||Age: ~1620Ma. Geological Province: Gawler Craton.||||||07-FEB-11
24502|St Peter Suite|63067|5|Briefly described|p2 Fig. 1|Paleoproterozoic|Paleoproterozoic|Age: ~1630Ma. Granite, granodiorite, adamellite, gneiss.||||||07-NOV-08
24502|St Peter Suite|63275|6|Mentioned|p13, p14 Fig.1, p18-20.|Late Paleoproterozoic|Late Paleoproterozoic|Deposition followed a period of convergent magmatism. MT modelling suggests this unit is part of the resistive core region of the Gawler Craton.||||||
24502|St Peter Suite|63866|5|Briefly described|p6, p9, p15, p18, p31|Statherian|Statherian|Nuyts Domain, Gawler Craton. U-Pb dates of 1619 +/- 15 Ma (TIMS, Fanning et al., 1997) and 1615+/- 8 Ma (SHRIMP, Fanning et al., 2007) are assigned to granites of this suite.|1620-1610 Ma (Flint et al., 1990)|||||
24502|St Peter Suite|64130|4|Described|p1377-1378, p1380 Fig.2  |Mesoproterozoic|Mesoproterozoic|See also p1382-1388 Fig.6, p1392. Unusual example of Australian Proterozoic suite that resembles modern subduction/arc-related magmatism.|c.1620-1610 Ma (Flint et al., 1990).|||Intrudes Nuyts Volcanics. Intruded by the Hiltaba Suite.|Granitic to mafic magmatic suite.|
24502|St Peter Suite|64576|6|Mentioned|p625, p625 Fig. 2|Mesoproterozoic|Mesoproterozoic|Age: 1630 and 1615Ma. Arc-like magmatism.||||||08-JUL-13
24502|St Peter Suite|64722|5|Briefly described|Fig. 2 p3-6, p14|Statherian|Statherian|Intermediate to felsic calcalkaline suite with geochemical characteristics indicative of a subduction-related magmatic arc depositional environment.|1620 - 1610 Ma.|||||11-APR-12
24502|St Peter Suite|64725|6|Mentioned|p58 Fig.2.|||Gawler Craton.||||||
24502|St Peter Suite|64739|6|Mentioned|p264 Fig.1, p265 Table 1. |Paleoproterozoic|Paleoproterozoic|Gawler Craton.|1630-1615 Ma.|||||08-JUL-13
24502|St Peter Suite|64740|4|Described|pp284-294.|Paleoproterozoic|Paleoproterozoic|Nuyts Domain, central Gawler Craton. 25,000 km2 intrusive magmatic rocks beneath sedimentary cover. Complex felsic to mafic magmatic relationships. Has medium-high K calc-alkaline composition related to subduction-related arc magmatism.|c.1620-1608 Ma.|||Intruded and overlain by Hiltaba Suite, Gawler Range Volcanics and Munjeela Granite.|Granite, granodiorite, dolerite; mafic dykes, gabbro bodies.|29-MAR-12
24502|St Peter Suite|64741|5|Briefly described|p299 Fig. 2|||||||||07-FEB-11
24502|St Peter Suite|64828|5|Briefly described|p1064 Fig. 1|Paleoproterozoic|Paleoproterozoic|Geological province: Gawler Craton.||||||04-MAR-09
24502|St Peter Suite|65375|6|Mentioned|p13.|Paleoproterozoic|Paleoproterozoic||c.1630 Ma.|||||
24502|St Peter Suite|65376|5|Briefly described|p8 Fig.1.1, p10, pp133-137. |Paleoproterozoic|Paleoproterozoic|Deformed co-magmatic granitoids in the central and southern Gawler Craton around 1620 Ma. Slightly younger than the 'associated' Nuyts Volcanics.|1622-1608 Ma.|||||
24502|St Peter Suite|65390|5|Briefly described|p22 Fig. 3, p21, p24|Statherian|Statherian|Nuyts Domain, Gawler Craton. Also spelt St Peters Suite in text. Tonalitic to granodioritic rocks intruded into the Nuyts Domain of the Gawler Craton at approx. 1630-1610 Ma. Has an arc-like geochemical signature.||||||
24502|St Peter Suite|65485|6|Mentioned|Fig 1|Paleoproterozoic|Paleoproterozoic|||||||19-MAR-12
24502|St Peter Suite|65772|5|Briefly described|p228, p229 Fig.2, p238|Statherian|Statherian|1620-1608 Ma. Mafic-felsic suite had been interpreted as forming in a subduction-related arc.||||||
24502|St Peter Suite|65922|6|Mentioned|p9, p13 Fig.4, p31|Statherian|Statherian|1635-1610 Ma. Granitic orthogneiss; calcalkaline, with mixed mafic and felsic magmas. Intrudes or is comagmatic with Nuyts Volcanics.||||||
24502|St Peter Suite|66299|6|Mentioned|p293.|||Younger granites in Durlacher Supersuite of Capricorn Orogen are of a similar age to granites of this Suite in the western Gawler Craton.||||||
24502|St Peter Suite|66302|5|Briefly described|p4-5 Figs.3,4; p19, p23-24, p55-56|Paleoproterozoic|Paleoproterozoic|Nuyts Domain, Gawler Craton. Granites of this suite have compositions similar in chemistry to Archean tonalite-trondhjemite-granodiorite suites and are interpreted to have formed by fractionation of a chemically-enriched mantle. See also p67-69, p71, p76 Fig.20, p90.  |ca. 1631-1608 Ma (Ferris and Schwarz, 2004)||||Granite, tonalite, granodiorite, diorite and gabbro.|
24502|St Peter Suite|66519|6|Mentioned|p32.|Paleoproterozoic|Paleoproterozoic|Gawler Craton.|1618-1608 Ma.|||Intruded by Point James Granite.|Granite; muscovite and garnet absent.|
24502|St Peter Suite|67058|6|Mentioned|p477 Fig. 1|Paleoproterozoic|Paleoproterozoic||1640-1620 Ma.|||||19-APR-12
24502|St Peter Suite|67112|6|Mentioned|p3 Fig.2|Paleoproterozoic|Paleoproterozoic|Gawler Craton.||||||
24502|St Peter Suite|67181|5|Briefly described|p616 Fig.1|Paleoproterozoic|Paleoproterozoic|Gawler Craton. References: Fairclough et al. 2003, Payne et al. 2003.|1640-1620 Ma|||||
24502|St Peter Suite|67323|5|Briefly described|Eastern Australia Time-Space Plot; p36|||A magmatic arc along the southern margin of the Gawler Craton. Apperas as St Peters Suite in the Time-Space Plot.|1620 +/- 4 Ma.|||||
24502|St Peter Suite|67536|5|Briefly described|Map Legend|Statherian|Statherian|Gawler Craton.|ca. 1620 +/- 4 Ma||||Granite to diorite, dolerite, amphibolite.|
24502|St Peter Suite|67581|6|Mentioned|p44 Fig.8, p45||||1620-1610 Ma.|||||
24502|St Peter Suite|67900|5|Briefly described|p20|Paleoproterozoic|Paleoproterozoic|Flint et al. (1990). SW Gawler Craton. Formed as a result of fractional crystallisation of an enriched mantle source with only minor crustal contamination.|c.1620-1608 Ma.||||Calc-alkaline affinities.|
24502|St Peter Suite|67980|6|Mentioned|p550|Statherian|Statherian||c.1610 Ma (Swain et al., 2008).|||||
24502|St Peter Suite|68131|5|Briefly described|p2 Fig.1|Paleoproterozoic|Paleoproterozoic||||||Granitic and felsic volcanic rocks.|
24502|St Peter Suite|69048|6|Mentioned|p3|||Central-western Eyre Peninsula.||||||
24502|St Peter Suite|69255|5|Briefly described|p788|Statherian|Statherian|Flint et al. (1990). Gawler Craton.|c.1620-1610 Ma.||||Granites.|
24502|St Peter Suite|69554|6|Mentioned|p128, 130|Paleoproterozoic|Paleoproterozoic|Central Gawler Craton.|c.1620-1608 Ma.|||||
24502|St Peter Suite|69649|5|Briefly described|p14-16, p6 Fig.4, p7, p8 Fig.6,  p36-38|Paleoproterozoic|Paleoproterozoic|See also p41, p42. Ages discussed. Volcanic-arc granites; calc-alkaline affinities. Variably deformed by Kararan Orogeny. SiO2 values range from gabbro to granite.|1630-1608 Ma.||||Granite to monzogranite; dolerite, diorite, amphibolite and lamprophyre dykes; monzogranite to granodiorite dykes; porphyritic monzogranite to granodiorite; pink porphyritic granite. A-type.|23-FEB-15
24502|St Peter Suite|70025|6|Mentioned|p22|Mesoproterozoic|Mesoproterozoic|Geological province: Mawson Craton.||||||
24502|St Peter Suite|70027|5|Briefly described|p56,58|Statherian|Statherian|Geological province: Gawler Craton. Emplaced into Gawler Craton ca. 1620-1610 Ma post-Kimban Orogeny.|ca. 1620-1610 Ma|||||
24502|St Peter Suite|70286|6|Mentioned|p884, 889|Paleoproterozoic|Paleoproterozoic|Western Gawler Craton.|1630-1608 Ma.|||||
24502|St Peter Suite|70337|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic||c.1630-1620 Ma.||||Granite, adamellite, granodiorite, diorite, pegmatite, amphibolite, dolerite, lamprophyre.|
24502|St Peter Suite|70511|6|Mentioned|p87|Paleoproterozoic|Paleoproterozoic|Gawler Craton.|1625-1615 Ma.|||||
24502|St Peter Suite|70738|6|Mentioned|p186|Paleoproterozoic|Paleoproterozoic|Southwest Gawler Craton. Formed in a magmatic arc setting.|c.1620 Ma.||||Granitoids.|
24502|St Peter Suite|70778|4|Described|p1, p5, p10, p24|Statherian|Statherian|Fowler Domain, Gawler Craton. 1607 Date derived from a sample in drillhole Nundroo 3 DDH 3. 1616 Date derived from a sample in drillhole Nundroo 2 DHH. Both SHRIMP dates are interpreted as magmatic crystallisation ages. Sampling,  petrography, zircon characteristics, SHRIMP analyses and results are discussed in detail.|1606 +/- 6 Ma 1616 +/- 5 Ma (SHRIMP U-Pb)||||Metamorphosed quartz diorite and garnet-bearing quartzo-feldspathic gneiss.|
24502|St Peter Suite|70858|6|Mentioned|p29, 31, 33|Paleoproterozoic|Paleoproterozoic|Gawler Craton. Regarded by the authors as a good candidate for 1.75 Ga and younger detrital zircons in the Wernecke Supersuite, Yukon.|1620-1610 Ma.|||||
24502|St Peter Suite|70893|4|Described|i, iii, iv, v, p1-p3, p8, p10|Statherian|Statherian|SHRIMP ages derived from this volume and are magmatic crystallisation ages. Previous age determinations detailed in addition to multiple ages from various samples of this suite. Associated with widespread alteration and mineralisation in the Gawler Cration. Geochemistry, petrography and lithology of multiple samples from this suite are described in detail. See also p18, p23, p26, p31, p36, p41, p42, p47, p53, p56, p78, p81-p83, p92.  |1633 +/- 4 Ma to 1608 +/- 7 Ma (SHRIMP)||||Bimodal magmatic plutons including granite, quartz diorite, granodiorite, diorite and gabbro.|
24502|St Peter Suite|70947|6|Mentioned|p960|Statherian|Statherian|Geological province: Gawler Craton.|ca. 1620 Ma|||||
24502|St Peter Suite|71037|6|Mentioned|p21 Fig.1|Paleoproterozoic|Paleoproterozoic|Shown only on 'Outcropping geology and mineral deposits of northern Eyre Peninsula' map p21 Fig.1.||||Shown as younger than Corunna Conglomerate.||
24502|St Peter Suite|71043|5|Briefly described|p104, p107|Statherian|Statherian|Flint et al. (1990). Gawler Craton.|1630-1604 Ma.|||||
24502|St Peter Suite|71169|5|Briefly described|p77|Statherian|Statherian|Gawler Craton.|c. 1620 Ma (Swain et al., 2008)||||Arc-like granitic rocks.|
24502|St Peter Suite|71317|4|Described|p1, p14-p16, p19, p175|Paleoproterozoic|Paleoproterozoic|Nuyts Domain, Gawler Craton. Together with the Peter Pan Supersuite and Tunkillia Suite forms the basement of the Peltabinna mapsheet.|1650-1605 Ma|||Overlain by the Gawler Range Volcanics.|Bimodal magmatic rocks.|
24502|St Peter Suite|71322|6|Mentioned|p136|Paleoproterozoic|Paleoproterozoic|Eastern Gawler Craton.||||||
24502|St Peter Suite|71341|6|Mentioned|p179 fig 1|Palaeoproterozoic|Palaeoproterozoic||ca. 1650 Ma|||||
24502|St Peter Suite|71348|6|Mentioned|p200|Statherian|Statherian|Geological province: Gawler Craton.|1630-1605 Ma|||||
24502|St Peter Suite|71534|5|Briefly described|p295-296,298, 301-302|Statherian|Statherian|Geological province: Gawler Craton. Magnesian and calc-alkaline with moderately evolved to relatively juvenile Sm-Nd isotopic compositions; indicating derivation in part from contemporary mantle in a possible subduction-related setting. Associated with renewed mantle input post-Kimban Orogeny. Formed in a continental magmatic arc (Swain et al., 2008).|c. 1630-1605 Ma|||||
24502|St Peter Suite|71559|6|Mentioned|p15 Fig 1, p16 Fig 2|Paleoproterozoic|Paleoproterozoic|Geological province: Gawler Craton.||||||
24502|St Peter Suite|71618|6|Mentioned|p135|Statherian|Statherian|Geological province: Gawler Craton. Possible, but unlikely source of ~1500-1800 Ma detrital zircons in the Madura Formation, Loongana Formation and Decoration Sandstone.|c. 1620 Ma|||||
24502|St Peter Suite|71712|6|Mentioned|p411, 419|Statherian|Statherian|Eastern Gawler Craton. Located west of the Cariewerloo Basin.|1620-1610 Ma||||Mafic to granitic rocks.|
24502|St Peter Suite|71859|5|Briefly described|p3, p4, p5, p6|Statherian|Statherian|Nuyts Domain, southern Gawler Craton. Ages are also derived after Symington et al., 2014; Reid et al., 2016.|1647-1608 Ma (Swain et al., 2008; Chalmers, 2009)||||Felsic to mafic, juvenile igneous rocks.|
24502|St Peter Suite|71862|5|Briefly described|p3-p4, p12, p21||||c. 1645-1610 Ma||||Felsic to mafic, juvenile intrusive rocks.|
24502|St Peter Suite|72090|6|Mentioned|p9-p10, p11, p14|Statherian|Statherian|Gawler Craton.|c. 1640-1610 Ma|||Overlain by the Gawler Range Volcanics.||
24502|St Peter Suite|72344|6|Mentioned|p5, p28|||Western Gawler Craton. Geochemically and isotopically similar to, and the same age as the Toolgana Supersuite.||||||
24502|St Peter Suite|72459|6|Mentioned|p6, p14, p21, p51|Mesoproterozoic|Paleoproterozoic|Bears similarities to 'Nicholls' garnet-bearing granitoids and 'Nicholls?'  biotite bearing granitoids north of Ceduna. Widespread in Nuyts Domain. High Mn levels are present.|1619 +/- 15 Ma, 1608 +/- 10 Ma.||||Granodiorite to granite.|
24502|St Peter Suite|72462|5|Briefly described|p1, p3, p6-7|Statherian|Statherian|Gawler Craton. I-type, calc-alkaline. Features complex mingling and mixing relationships. Interpreted as a volcanic arc system at a subduction margin but does not have an arc-like linear morphology. Hosts Ag-Pb mineralisation at Point Brown. [Age range written as 1620-1610 Ma and 1620-1615 Ma].|ca 1620-1610 Ma||||Comagmatic intrusive rocks including monzonite, granite, granodiorite, diorite, dolerite, amphibolite and lamprophyre.|
24502|St Peter Suite|72465|6|Mentioned|p10|||Western Gawler Craton. Is similar in age, geochemistry and isotopes with the Toongana Supersuite (Coompana Province).||||||
24502|St Peter Suite|72466|6|Mentioned|p10|||Western Gawler Craton. Has the same age, and similar geochemistry and isotopes, as Toolgana Supersuite in Coompana Province.||||||
24502|St Peter Suite|72468|6|Mentioned|p10|||Gawler Craton, western. Same age as, and is geochemically and isotopically similar to Toolgana Supersuite.||||||
24502|St Peter Suite|72469|6|Mentioned|p10|||Gawler Craton, western. Same age as, and is geochemically and isotopically similar to Toolgana Supersuite.||||||
24502|St Peter Suite|72470|6|Mentioned|p10|||Gawler Craton, western. Same age as, and is geochemically and isotopically similar to Toolgana Supersuite.||||||
24502|St Peter Suite|72471|6|Mentioned|p10|||Gawler Craton, western. Same age as, and is geochemically and isotopically similar to Toolgana Supersuite.||||||
24502|St Peter Suite|72472|6|Mentioned|p10|||Gawler Craton, western. Same age as, and is geochemically and isotopically similar to Toolgana Supersuite.||||||
24502|St Peter Suite|72947|6|Mentioned|p7|||Gawler Craton, southern. Similar in age and composition to the Koomalboogurra Suite. [Saint spelt St in text].||||||
24502|St Peter Suite|72949|6|Mentioned|p33-38|Statherian|Statherian|Gawler Craton, southwest. [Written as St Peter Suite]. Mantle Nd isotopic compositions/signatures. eNd(1620 Ma) = -3.7 to 3.7 (Swain et al., 2008; Reid et al., 2019). Considered to be arc magmatism.|ca. 1.647-1.604 Ga|||||
24502|St Peter Suite|73026|5|Briefly described|p4 fig1.2, p6, p9-10|Paleoproterozoic|Paleoproterozoic|Central/western Eyre Peninsula; Southwestern Gawler Craton. Rocks are characteristically juvenile with pronounced Nb and Ti anomalies, marked Y depletion, moderate to high Sr. Could reflect a continental magmatic arc or, alternatively I-type magamatism derived partly from metasomatised subcontinental lithospheric mantle.|c. 1620-1608 Ma|||Intrudes the Nuyts Volcanics.|Granite to diorite, dolerite and amphibolite.|
24502|St Peter Suite|73027|5|Briefly described|p4, p6, p9-10|Palaeoproterozoic|Palaeoproterozoic|Felsic and mafic rocks are characteristically juvenile with pronounced Nb and Ti anomalies, marked Y depletion, moderate to high Sr.|c. 1620 -1606 Ma||||Granite to diorite, dolerite and amphibolite.|
24502|St Peter Suite|73030|6|Mentioned|p2148-2150|Statherian|Statherian|Gawler Craton.|ca. 1620 to 1608 Ma|||||
24502|St Peter Suite|73084|6|Mentioned|p103-104, p123, p137|Statherian|Statherian|Gawler Craton southern and western edge. May represent westward-migrating arcs.|c. 1633 to 1608 Ma|||||
24502|St Peter Suite|73130|6|Mentioned|[poster]|Statherian|Statherian|Intrusion occurred prior to formation of the Itiledoo Basin. Age also written as c.1635-1610 Ma.|c. 1635-1605 Ma||||Intrusive rocks.|
24502|St Peter Suite|73155|6|Mentioned|p264 Fig.1|Statherian|Statherian|Gawler Craton.|ca. 1647-1604 Ma|||||
24502|St Peter Suite|73162|6|Mentioned|p449, Fig.1, p459, p461|Paleoproterozoic|Paleoproterozoic|Saint is spelt St in text.|1635-1605 Ma|||||
24502|St Peter Suite|73165|6|Mentioned|p621|Statherian|Statherian|Gawler Craton. Associated with juvenile mantle input resulting in wide-spread crustal melting and intense magmatism including the Gawler Range Volcanics and Hiltaba Suite.|ca 1640-1608 Ma|||||
24502|St Peter Suite|73224|5|Briefly described|p42|||Southern Gawler Craton. Similar in age and composition to the Koomalboogurra Suite. Interpreted to represent subduction-related granites that developed on the edge or outboard of the Gawler Craton.||||||
24502|St Peter Suite|73233|5|Briefly described|p26, p27 Fig.1, p28-31|Paleoproterozoic|Paleoproterozoic|Gawler Craton, Nyuts Domain and eastern Fowler Domain. Deformed and metamorphosed in eastern Fowler Domain, moderately to highly magnetic.|1607+/-6 Ma, 1616+/-5 Ma|||Intruded by Hiltaba Suite|Igneous Intrusions. Includes metamorphosed quartz diorite and garnet-bearing quartzo-feldspathic gneiss.|
24502|St Peter Suite|73234|6|Mentioned|p19|Statherian|Statherian|Eyre Peninsula, north-western. Age from Reid et al. (2019).|c. 1630-1610 Ma||||Igneous rocks.|
24502|St Peter Suite|73235|6|Mentioned|p52-53, p63|Statherian|Statherian|Gawler Craton. Nuyts, Cleve and Coulta regions. Hosts gold mineralisation in the Western Gawler and Tunkillia mineral fields of the Kararan (Hiltaba Suite) gold mineral system.|1630-1608 Ma|||||
24502|St Peter Suite|73252|3|Fully described|p4-6, p8, p10|Statherian|Statherian|Gawler Craton. Bimodal magmatic system. Distinct geochemistry to other Proterozoic magmatic suites of the region. Isotopically juvenile; represents an addition of mantle material into the crust. Interaction of mafic and felsic magmas common throughout the suite. Largest onshore surface exposures occur between Slade Point (south of Streaky Bay) to west of Point James. Three magmatic systems were identified: 1) a magma transfer zone where various felsic and mafic magmas interacted, 2) a felsic magma chamber with minor comagmatic mafic magmas, and 3) a mafic magma chamber [see article for detailed field descriptions]. Thought to be related to subduction zone processes, which has implications for mineral endowment. Emplaced into a contractional tectonic setting. Based on exposed rock types, current erosion level is interpreted to dissect deeper than the crustal levels that typically host porphyry Cu-Au deposits.|1647-1604 Ma[?]||||Texturally and mineralogically heterogeneous; dominantly felsic with less common intermingled and isolated mafic rocks such as coarse to very coarse pyroxene-rich cumulates and also includes magmatic breccia.|
24502|St Peter Suite|73256|4|Described|p557-562, p564-576|Statherian|Statherian|Gawler Craton. Subduction-related continental magmatic arc setting. Compressional deformation. Complex system that formed from the mingling of felsic and mafic magmas. May have mineral potential. [See article for petrographic descriptions, whole-rock geochemistry, and zircon morphological and compositional characterisation].|ca 1633-1608 Ma|||||
24502|St Peter Suite|73302|5|Briefly described|p31-40, 44-54|Palaeoproterozoic|Palaeoproterozoic|SW Gawler Craton. Comprises most of the Nuyts Domain; occupies up to 25,000 km2, largely thinly buried. Physical magma processes, deformation, geochronology, geochemistry discussed in detail.|c.1633 Ma to 1608 Ma.|||Coeval with Saint Francis Granite and Nuyts Volcanics.|From quartz monzonite, granite, granodiorite, tonalite and diorite to gabbro and pyroxenite.|
24502|St Peter Suite|73493|5|Briefly described|p712, p714 Fig.1, p716 Fig.3|Statherian|Statherian|Gawler Craton.|ca 1635-1605 Ma||||Granitic, and mafic.|
26147|Stairway Sandstone|9814|5|Briefly described|Map Legend|Ordovician|Ordovician|Of the Larapinta Group. Fossiliferous sandstone, silty sandstone.||||||
26147|Stairway Sandstone|12891|5|Briefly described|p733|Middle Ordovician|Middle Ordovocian|Geological province: Amadeus Basin. Similar to the fossiliferous sandstones of Hansons River Beds.||||||07-FEB-11
26147|Stairway Sandstone|13995|5|Briefly described|p69, p73, p75, p79, p90, p101, p103|Middle Ordovician|Middle Ordovician|Amadeus Basin. Brachiopod, rostroconch, pelecypod species. Nautiloids mentioned; contemporary fauna occur in the Coolibah Formation (Georgina Basin). At Mount Watt, this unit has the type locality for Arandaspis prionotolepis and Porophoraspis crenulata, the first record of Ordovician vertebrates (armoured agnathans) in the Southern Hemisphere.||Larapinta Group.||Conformably overlies Horn Valley Siltstone. Is overlain conformably by Stokes Siltstone.|The middle unit of this formation contains phosphorite layers and red beds.|
26147|Stairway Sandstone|22560|4|Described|p5|Late Ordovician|Ordovician|||||||
26147|Stairway Sandstone|22561|6|Mentioned|p23|Neoproterozoic|Neoproterozoic|also see Stairway Formation p9||||||
26147|Stairway Sandstone|22565|5|Briefly described|p71 & Table 1||Ordovician|Thickness at Areyonga Creek measured from surface expression - 250m thick.  Approx. thickness measured from seismic data - 310m.||||||
26147|Stairway Sandstone|22566|5|Briefly described|p85|Ordovician|Early Ordovician|Of the Larapinta Group.||||||04-DEC-06
26147|Stairway Sandstone|22646|5|Briefly described|p105|Ordovician|Ordovician|||||||
26147|Stairway Sandstone|22650|4|Described|p 160|Ordovician|Ordovician|Of the Larapinta Group.||||||04-DEC-06
26147|Stairway Sandstone|22651|6|Mentioned|Fig 10 btw p182-183|Ordovician|Ordovician|||||||
26147|Stairway Sandstone|22655|5|Briefly described|p 273|||informally divided into upper and lower Stairway Sandstone p253.||||||04-DEC-06
26147|Stairway Sandstone|22656|4|Described|p 278|Early Ordovician|Early Ordovician|||||||
26147|Stairway Sandstone|22758|6|Mentioned|Fig 2 on p305|||Max Age - late Arenig||||||
26147|Stairway Sandstone|22759|6|Mentioned|p318|||Informally divided into upper and lower Stairway Sandstone.||||||04-DEC-06
26147|Stairway Sandstone|22763|6|Mentioned|p400||Early Ordovician|Of the Larapinta Group.||||||04-DEC-06
26147|Stairway Sandstone|22804|6|Mentioned|p452|Ordovician|Ordovician|Of the Larapinta Group.||||||04-DEC-06
26147|Stairway Sandstone|22805|4|Described|p470-471||Ordovician|Shown to be a secondary reservoir p468.  Informally divided into upper and lower Stairway Sandstone p471.||||||04-DEC-06
26147|Stairway Sandstone|22806|4|Described|p485|Ordovician|Ordovician|Informally divided into upper and lower Stairway Sandstone p480.||||||04-DEC-06
26147|Stairway Sandstone|22807|4|Described|p499-503|Ordovician|Ordovician|Parent - Larapinta Group.  The Stairway Sandstone has been divided into upper, middle and lower subunits see p499.||||||04-DEC-06
26147|Stairway Sandstone|22823|6|Mentioned|p512|||||||||
26147|Stairway Sandstone|22824|4|Described|p526 and p530-531|Ordovician|Cambrian|Of the Larapinta Group.  Age range of Llavirnian to Llandelian, corresponding to an absolute age of 478-458 Ma.  see p526.||||||04-DEC-06
26147|Stairway Sandstone|22825|6|Mentioned|p544|Ordovician|Ordovician|||||||
26147|Stairway Sandstone|22826|4|Described|p574|Ordovician|Ordovician|Of the Larapinta Group.||||||04-DEC-06
26147|Stairway Sandstone|23361|5|Briefly described|16 Fig.4|Cambrian|Cambrian|||||||
26147|Stairway Sandstone|23818|6|Mentioned|p111|||Geological Province: Amadeus Basin.||||||
26147|Stairway Sandstone|24063|5|Briefly described|p220|Ordovician|Cambrian|Geological Province: Amadeus Basin.||||||
26147|Stairway Sandstone|24064|5|Briefly described|p229 Fig.7|Ordovician|Ordovician|Of Larapinta Group. Geological Province: Amadeus Basin.||||||
26147|Stairway Sandstone|24301|4|Described|p20|Ordovician|Ordovician|Of Larapinta Group. Originally defined as Stairway Greywacke (Prichard and Quinlan, 1962).  See also Stairway sandstone on p7 Tb.2. Max. thickness: 600m.  Overlies Inindia beds, underlies Stokes Siltstone.  Geological Province: Amadeus Basin.||||||31-MAR-09
26147|Stairway Sandstone|29721|6|Mentioned|Table 44|||||||||
26147|Stairway Sandstone|29972|6|Mentioned|Table 1|||||||||
26147|Stairway Sandstone|30238|4|Described|p68|||Cambrian - Ordovician age||||||
26147|Stairway Sandstone|30258|6|Mentioned|Fig.2|||Ordovician age. Part of Larapinta Group.||||||
26147|Stairway Sandstone|30540|6|Mentioned|p61|||Reservoir rock of secondary importance||||||
26147|Stairway Sandstone|30544|6|Mentioned|p49|||||||||
26147|Stairway Sandstone|30615|6|Mentioned|p177|||Reservoir rock of secondary importance||||||
26147|Stairway Sandstone|30659|6|Mentioned|p89|||Palaeomagnetism. Middle Ordovician age||||||
26147|Stairway Sandstone|30660|6|Mentioned|Table 1|||Middle Ordovician age||||||
26147|Stairway Sandstone|30661|6|Mentioned|Table 1|||||||||
26147|Stairway Sandstone|30662|6|Mentioned|p188|||Palaeomagnetic dates||||||
26147|Stairway Sandstone|30983|5|Briefly described|p75|||||||||
26147|Stairway Sandstone|31566|6|Mentioned|p231|||See also Fig. 2||||||
26147|Stairway Sandstone|31567|6|Mentioned|p276|||Overlain unconformably by Polly Conglomerate.||||||04-DEC-06
26147|Stairway Sandstone|31707|4|Described|p53|||Lithology||||||
26147|Stairway Sandstone|32208|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
26147|Stairway Sandstone|32209|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
26147|Stairway Sandstone|32854|6|Mentioned|p351|||Stratigraphy p352.||||||04-DEC-06
26147|Stairway Sandstone|33307|6|Mentioned|Fig.6|||||||||
26147|Stairway Sandstone|33625|6|Mentioned|Table 2|||||||||
26147|Stairway Sandstone|33738|6|Mentioned|p52|||||||||
26147|Stairway Sandstone|33761|6|Mentioned|p146|||Ordovician. Of the Larapinta Group.||||||04-DEC-06
26147|Stairway Sandstone|33832|6|Mentioned|p8|||Stratigraphy||||||
26147|Stairway Sandstone|33971|4|Described|p28|||Of the Larapinta Group.||||||04-DEC-06
26147|Stairway Sandstone|34111|5|Briefly described|Table 2|||Cambrian - Ordovician. See also pp4,15,17-19.||||||04-DEC-06
26147|Stairway Sandstone|34280|6|Mentioned|p10|||||||||
26147|Stairway Sandstone|34442|5|Briefly described|Table 1|||Cambrian - Ordovician||||||
26147|Stairway Sandstone|34580|4|Described|Table 1|||Ordovician||||||
26147|Stairway Sandstone|34612|6|Mentioned|p111|||Correlation. Ordovician. Amadeus Basin.||||||
26147|Stairway Sandstone|34722|6|Mentioned|p288|||||||||
26147|Stairway Sandstone|35088|6|Mentioned|Fig.8|||||||||
26147|Stairway Sandstone|35102|6|Mentioned|Fig.2|||||||||
26147|Stairway Sandstone|36096|6|Mentioned|p219|||||||||
26147|Stairway Sandstone|36331|6|Mentioned|p53|||||||||
26147|Stairway Sandstone|36818|6|Mentioned|p203|||||||||
26147|Stairway Sandstone|36821|6|Mentioned|p398|||||||||
26147|Stairway Sandstone|37818|6|Mentioned|Table 2|||||||||
26147|Stairway Sandstone|39213|6|Mentioned|Fig.6|||Amadeus Basin Succession||||||
26147|Stairway Sandstone|40136|5|Briefly described|p39|||See also p18 and p23.||||||04-DEC-06
26147|Stairway Sandstone|40137|6|Mentioned|Table 1|||||||||
26147|Stairway Sandstone|40740|3|Fully described|p54|||Mention p6.||||||04-DEC-06
26147|Stairway Sandstone|40810|4|Described|p10|||||||||
26147|Stairway Sandstone|40852|6|Mentioned|p34|||||||||
26147|Stairway Sandstone|40910|6|Mentioned|p13|||||||||
26147|Stairway Sandstone|40911|6|Mentioned|Map legend|Ordovician|Ordovician|Prob. Ordovician||||||
26147|Stairway Sandstone|40926|6|Mentioned|p11|||||||||
26147|Stairway Sandstone|41039|4|Described|p6|||Mention p13.||||||04-DEC-06
26147|Stairway Sandstone|41115|6|Mentioned|Fig.2|||||||||
26147|Stairway Sandstone|41190|5|Briefly described|p267|||||||||
26147|Stairway Sandstone|41203|5|Briefly described|p13|||||||||
26147|Stairway Sandstone|41224|6|Mentioned|p428|||||||||
26147|Stairway Sandstone|41270|6|Mentioned|Table 1|||||||||
26147|Stairway Sandstone|41385|6|Mentioned|Fig.2|||||||||
26147|Stairway Sandstone|41621|5|Briefly described|Map legend|Early Ordovician||||||||
26147|Stairway Sandstone|41708|6|Mentioned|p206|||||||||
26147|Stairway Sandstone|41711|6|Mentioned|p259|||||||||
26147|Stairway Sandstone|41717|6|Mentioned|p355|||||||||
26147|Stairway Sandstone|41723|6|Mentioned|Map legend|Ordovician||||||||
26147|Stairway Sandstone|41819|6|Mentioned|Map legend|Early Ordovician||||||||
26147|Stairway Sandstone|41820|3|Fully described|p11|||||||||
26147|Stairway Sandstone|42037|5|Briefly described|Table 3 P79|||||||||
26147|Stairway Sandstone|42049|6|Mentioned|p220|||||||||
26147|Stairway Sandstone|42059|6|Mentioned|p132|||See also Fig.2||||||
26147|Stairway Sandstone|42060|6|Mentioned|Fig.5 P140|||||||||
26147|Stairway Sandstone|42082|4|Described|p323|||See also Fig.3||||||
26147|Stairway Sandstone|42354|6|Mentioned|Fig.3 P5, P6|||||||||
26147|Stairway Sandstone|42504|5|Briefly described|p77|||||||||
26147|Stairway Sandstone|42699|5|Briefly described|map legend|Ordovician||||||||
26147|Stairway Sandstone|42940|5|Briefly described|Plate 8|||||||||
26147|Stairway Sandstone|43035|5|Briefly described|p21|||Of Larapinta Group.||||||04-DEC-06
26147|Stairway Sandstone|43105|5|Briefly described|p8|||||||||
26147|Stairway Sandstone|43225|5|Briefly described|Map Legend||Ordovician|Of Larapinta Group.||||||04-DEC-06
26147|Stairway Sandstone|43230|6|Mentioned|p9||Ordovician|Reservoir target.||||||
26147|Stairway Sandstone|43503|6|Mentioned|p11-50|Darriwilian|Yapeenian|||||||11-JUL-16
26147|Stairway Sandstone|43646|6|Mentioned|Fig.3,p554||Darriwilian|||||||
26147|Stairway Sandstone|43647|6|Mentioned|p531|||||||||
26147|Stairway Sandstone|43648|6|Mentioned|Fig.1,p488|||||||||
26147|Stairway Sandstone|43649|6|Mentioned|p453||Ordovician|||||||
26147|Stairway Sandstone|43803|6|Mentioned|Fig.5,p71|||||||||
26147|Stairway Sandstone|44133|5|Briefly described|p40, 43, 4 Fig. 7.2|Late Ordovician|Middle Ordovician|Geological Province: Western Warburton Basin. Of the Larapinta Group.||||||
26147|Stairway Sandstone|44323|14|Not recorded|map legend||Ordovician|SG/53-6. Ordovician.||||||
26147|Stairway Sandstone|44342|4|Described|p.6, Table 2||Ordovician|SG/53-5. U-M Ordovician.||||||
26147|Stairway Sandstone|44343|14|Not recorded|map legend||Late Ordovician|U.Ordovician.||||||
26147|Stairway Sandstone|44395|14|Not recorded|p.8,9,10,13, Tb.2||Ordovician|||||||
26147|Stairway Sandstone|44396|5|Briefly described|map legend|||(Camb-Ord). Of Larapinta Group.||||||04-DEC-06
26147|Stairway Sandstone|44402|5|Briefly described|map legend|Ordovician|Cambrian|Part of Larapinta Group. Camb-Ord.||||||02-DEC-04
26147|Stairway Sandstone|44433|14|Not recorded|map legend|||Cambrian to Ordovician.||||||
26147|Stairway Sandstone|44484|14|Not recorded|p.4,8,11,12,13, Tb.1|||(Camb-Ord).||||||
26147|Stairway Sandstone|44485|14|Not recorded|map legend|Ordovician|Cambrian|Part of Larapinta Group. Camb-Ord.||||||
26147|Stairway Sandstone|44495|4|Described|p.6, map||Ordovician|AYERS ROCK sheet (G52-8). See p.8,10,11, for details. Middle-Upper Ordovician.||||||04-DEC-06
26147|Stairway Sandstone|44496|5|Briefly described|map legend||Ordovician|White fine sandstone and kaolititic sandstone, minor siltstone.||||||02-DEC-04
26147|Stairway Sandstone|44497|4|Described|p.11, Table 2|Ordovician|Cambrian|SF/53-13. Cambrian-Ord.||||||
26147|Stairway Sandstone|44498|14|Not recorded|map legend|Ordovician|Cambrian|Part of Larapinta Group. Camb-Ord.||||||22-DEC-09
26147|Stairway Sandstone|44505|14|Not recorded|p.5,8,10, Table 1|Ordovician|Cambrian|Of Larapinta Group. Camb-Ord.||||||
26147|Stairway Sandstone|44506|14|Not recorded|map legend|Ordovician|Cambrian|Cambrian to Ordovician.||||||
26147|Stairway Sandstone|45036|2|Defined|p3|Middle Ordovician|Middle Ordovician|See also p4-61||||||04-DEC-06
26147|Stairway Sandstone|45041|4|Described|p71|||See also pp72-78. Middle Ord.||||||04-DEC-06
26147|Stairway Sandstone|45115|6|Mentioned|p7|||||||||
26147|Stairway Sandstone|45118|6|Mentioned|p1,3|||||||||
26147|Stairway Sandstone|45148|6|Mentioned|Fig.4|||See also p18.||||||04-DEC-06
26147|Stairway Sandstone|45155|6|Mentioned|Fig.8|||||||||
26147|Stairway Sandstone|45170|6|Mentioned|p8|||||||||
26147|Stairway Sandstone|46740|14|Not recorded|p.187|||Phosphate.||||||
26147|Stairway Sandstone|46841|6|Mentioned|p106|||||||||
26147|Stairway Sandstone|46928|6|Mentioned|p323|||See also Table 1.||||||
26147|Stairway Sandstone|47050|6|Mentioned|p240|||||||||
26147|Stairway Sandstone|47052|6|Mentioned|p261|||||||||
26147|Stairway Sandstone|48639|4|Described|p.13||Ordovician|See also page, 77,11,13,16. Mising in section in Alice No.1. (G55-2).||||||
26147|Stairway Sandstone|48862|14|Not recorded|p.15||Early Ordovician|On many pages. p.8,15,18,24-28,40,43; opp.8,9; Pl.4,9-11. L.-M.Ord. Supersedes 'Stairway Greywacke'. (F52-15).||||||04-DEC-06
26147|Stairway Sandstone|48863|2|Defined|p.27||Ordovician|Tb.1. opp.p.7,9,10,16,19,20,24,28,29,40-42,Pl.4,5,6,11,13,15,16. Middle Ordovician. (G52-4,G53-1).||||||
26147|Stairway Sandstone|48864|14|Not recorded|p.32, Pl.13|||Now called Stairway Greywacke (?). (G52-8).||||||04-DEC-06
26147|Stairway Sandstone|48865|2|Defined|p.5,10,Fig.23||Ordovician|Many figures. Fig.4,22,15,45,46,49,50,Pl.1,2,7,9,10. Unit of Larapinta Gp. (G52-8,G53-5,6).||||||
26147|Stairway Sandstone|48890|4|Described|p.46||Ordovician|See also Tables, Figs and Plates. of the Larapinta Group.||||||04-DEC-06
26147|Stairway Sandstone|48963|6|Mentioned|p2|||||||||
26147|Stairway Sandstone|50089|5|Briefly described|p430 Fig. 5|Ordovician|Ordovician|Geological Province: Amadeus Basin.||||||04-MAY-05
26147|Stairway Sandstone|50098|5|Briefly described|p1, p3 Fig. 2|||Of the Larapinta Group. Geological Province: Amadeus Basin.||||||
26147|Stairway Sandstone|60674|5|Briefly described|Map legend|Ordovician|Ordovician|Of the Larapinta Group. Thinly bedded, fine to medium clean sandstone; minor minor interbedded sandy limestone, coarse sandstone, medium silty sandstone, phophorite. Geological Province: Amadeus Basin.||||||
26147|Stairway Sandstone|61309|5|Briefly described|p16 Fig. 4|||Geological Province: Amadeus Basin.||||||06-FEB-08
26147|Stairway Sandstone|61385|5|Briefly described|Map legend|Ordovician|Ordovician|Sandstone, siltstone, limestone; fossiliferous. Geological Province: Amadeus Basin.||||||
26147|Stairway Sandstone|61387|5|Briefly described|Map legend|Ordovician|Ordovician|Of the Larapinta Group. Sandstone, siltstone, limestone; marine fossils. Geological Province: Amadeus Basin.||||||
26147|Stairway Sandstone|61518|5|Briefly described|Map Legend|Ordovician|Ordovician|Of the Larapinta Group. Thin bedded fine to medium grained clean sandstone; minor interbedded sandy limestone, coarse sandstone, medium grained silty sandstone, phosporite. Geological Province: Amadeus Basin.||||||
26147|Stairway Sandstone|61519|5|Briefly described|Map Legend|Ordovician|Ordovician|Of the Larapinta Group. Sandstone, siltstone, limestone; marine fossils. Geological Province: Amadeus Basin.||||||
26147|Stairway Sandstone|62359|6|Mentioned|p547 Fig. 7|||Geological Province: Amadeus Basin. See also the misspelt(?) Stairways Sandstone. ||||||
26147|Stairway Sandstone|62376|5|Briefly described|p18|Early Ordovician|Early Ordovician|Of the Larapinta Group. Geological Province: Amadeus Basin.||||||09-FEB-10
26147|Stairway Sandstone|62379|5|Briefly described|p7 Fig. 2|Ordovician|Ordovician|Of the Larapinta Group. Geological Province: Amadeus Basin.||||||
26147|Stairway Sandstone|62595|6|Mentioned|p28 Fig.4.|Early Ordovician|Early Ordovician|Amadeus Basin. Relative probability plots of detrital zircon data are shown.||||||
26147|Stairway Sandstone|62794|5|Briefly described|p288, 289, 290, p291-292, 299, 336, 337|Early Ordovician|Early Ordovician|Unit in Larapinta Group. Unconformably overlies Horn Valley Siltstone and underlies Stokes Siltstone. Two cliff-forming, resistant sandstone units separated by fine clastics, phosphorites and carbonates. Base of the unit is fossiliferous.||||||
26147|Stairway Sandstone|62795|6|Mentioned|p347, p348|Ordovician|Middle Ordovician|In Amadeus Basin. Basal fauna including Prosopiscus tatei and conodonts are dated as early Darriwilian Stage. This correlates with the middle part of Rowena Formation, Mutawintji Group, western NSW.||||||
26147|Stairway Sandstone|62982|5|Briefly described|p7|Llanvirnian|Llanvirnian|Of the Larapinta Group. Shallow-marine deposits. Overlies Horn Valley Siltstone; overlain by Stokes Siltstone. Geological Province: Amadeus Basin.||||||16-JAN-07
26147|Stairway Sandstone|63562|4|Described|p338 fig 3, p352 fig 10, p353, p347-9|Early Ordovician|Early Ordovician|Of Amadeus Basin. Mixed aged zircons, similar to Pacoota Sandstone and Tomahawk Formation: a third were 0.65-0.5 Ga.||Larapinta Group.||Overlies Horn Valley Siltstone. Is overlain by Stokes Siltstone.|Well-sorted, fine-grained quartz sandstone with cross beds and ripple marks; abundant body fossils.|
26147|Stairway Sandstone|64068|6|Mentioned|p77, 226|||Of Amadeus Basin. Correlated with Nora Formation, Georgina Basin.||||||
26147|Stairway Sandstone|64334|5|Briefly described|p39-41, 43, 45, 47|Ordovician|Ordovician|Amadeus Basin. Appears as Stairway Siltstone on p39. Reservoir rock.||Larapinta Group.||Unconformably overlies Horn Valley Siltstone. Is overlain by Stokes Siltstone.|Shallow-marine sandstone.|
26147|Stairway Sandstone|64778|6|Mentioned|p13, 17, 20-21, 27-28|Ordovician|Ordovician|Amadeus and Pedirka Basins.||||Overlies Horn Valley Siltstone.||
26147|Stairway Sandstone|64809|5|Briefly described|p2, p3 Fig.2, p6 Fig.4, p11 Fig.10|Middle Ordovician|Middle Ordovician|See also p13 Fig.13. Deposition on an open shelf in well-oxygenated waters.||Of the Larapinta Group||||
26147|Stairway Sandstone|65233|3|Fully described|p3 Fig. 2, p10|Early Ordovician|Early Ordovician|Of lower Larapinta Group. Conformable on/gradational with Stairway Sst; gradational below Stokes Siltstone. Max. thickness: 550m decreasing east, west and south. Geological province: Amadeus Basin. Tripartite lithology - details included.||||||07-FEB-11
26147|Stairway Sandstone|65309|6|Mentioned|p14.|Ordovician|Ordovician|Angular clasts occur in Langra Formation.||||||
26147|Stairway Sandstone|65342|6|Mentioned|p3.|||Amadeus Basin. Max. thickness at least 109 m.||||Overlies Horn Valley Siltstone (equivalent). Is overlain by Mereenie Sandstone.||
26147|Stairway Sandstone|65489|5|Briefly described|p125|Ordovician|Ordovician|Amadeus Basin. Hosts the Mereenie Mount Wikter 1 (and others) oil and gas shows.||Unit in Larapinta Group.||Overlies Horn Valley Siltstone. Is overlain by Stokes Siltstone.||
26147|Stairway Sandstone|66623|6|Mentioned|p446.|Ordovician|Ordovician|Amadeus Basin. Contains Darriwilian age Prosopiscus tatei, and Arandaspis sp. impression, both of which occur in upper Rowena Formation, Koonenberry Belt.||||||
26147|Stairway Sandstone|67326|5|Briefly described|p2-4|Early Ordovician|Early Ordovician|Amadeus Basin.||Larapinta Group.||Overlies Horn Valley Siltstone. Is overlain by Stokes Siltstone.||
26147|Stairway Sandstone|67565|5|Briefly described|p41, p50, p51.|Middle Ordovician|Middle Ordovician|Amadeus Basin. Forms prominent ridges. Up to 460 m thick. Contains fossils of the agnathan Porophoraspis, as well as trilobites, nautiloids, pelecypods, fish and ichnofauna. One of the reservoirs in the Mereenie oil/gas field; an abundance of oil-stained core in the Mount Winter-2A well. Contains pelletal phosphate occurrences, but they are too thin and low grade to be economic.|||||Thinly-bedded, fine- to medium-grained clean sandstone with minor interbedded sandy limestone, grey siltstone, coarse sandstone and purple-brown, medium silty sandstone; local phosphorite and phosphatic sandstone.|
26147|Stairway Sandstone|67856|6|Mentioned|p338 fig 4-30|Late Ordovician|Early Ordovician|||Of Larapinta Group.||||
26147|Stairway Sandstone|68297|5|Briefly described|p177|Llanvirn|Arenig|Amadeus Basin. Includes first complete Ordovician vertebrates from Australasia||||||
26147|Stairway Sandstone|68316|6|Mentioned|p778 Fig.1|||||||||
26147|Stairway Sandstone|68323|6|Mentioned|p4 Fig.2|Early Ordovician|Early Ordovician|Amadeus Basin.||Larapinta Group.||||
26147|Stairway Sandstone|69418|5|Briefly described|p3:36|Ordovician|Ordovician|Amadeus Basin. Hosts the Mereenie (oil and gas) and the Palm Valley (gas) fields. Has unconventonal petroleum potential (tight gas).||||||12-JUL-16
26147|Stairway Sandstone|69437|5|Briefly described|p22:10, 15|Ordovician|Ordovician|Amadeus Basin. Has considerable unconventional petroleum potential: tight gas.||||Overlies Horn Valley Siltstone. Is overlain by Stokes Siltstone.||12-JUL-16
26147|Stairway Sandstone|69438|4|Described|p23:2-3, 7, 10, 20, 34-36, 53-57, 59-61|Middle Ordovician|Middle Ordovician|Pritchard and Quinlan (1965). Amadeus Basin. Thickens northwards up to 544m. The bottom unit has basal pyritic ooids and a thin quartz pebble layer at top. Contains abundant fossils (listed). Deposited in a broad E-W oriented epicontinental seaway. Darriwilian to early Gisbornian age. Hosts malachite at the Boggy Hole Cu occurrence, and pelletal phosphate rock at several locations (briefly described). One of the main hydrocarbon reservoirs for the Basin; sealed by thick shales of Stokes Siltstone.||Larapinta Group.||Unconformably/disconformably overlies Horn Valley Siltstone, Winnall beds and Bitter Springs Formation. Is overlain conformably and gradationally by Stokes Siltstone.|Prominent massively bedded quartzic sandstone; overlain by thinly bedded sandstone with local residual phosphatic gravels, thin limestone, black shale and siltstone; quartzic sandstone with interbeds of mudstone, siltstone and phosphorites at top.|12-JUL-16
26147|Stairway Sandstone|69443|6|Mentioned|p28:27|||Amadeus Basin.||||Correlated with Toko Group.||12-JUL-16
26147|Stairway Sandstone|69447|6|Mentioned|p32:5|||Amadeus Basin. Contains fossils with affinities to Hanson River beds (Wiso Basin).||||||12-JUL-16
26147|Stairway Sandstone|69449|6|Mentioned|p34:2 Fig.34.2; 34:4|Ordovician|Ordovician|Eastern Amadeus Basin.||||Probable correlative of Innamincka Formation.||12-JUL-16
26147|Stairway Sandstone|69673|4|Described|p66, p79, p87, p89, p92, p96, p103, |Ordovician|Cambrian |Maximum thickness of 544m. Main reservoir in surprise oil field.||Larapinta Group||disconformably overlies Horn Valley Siltstone, conformably overlain by Stokes Siltstone, Unconformably overlies Pertaoorrta Group|Massively bedded quartzic sandstone and thinly bedded sandstone with minor black shale, siltstone and thin limestone layers.|
26147|Stairway Sandstone|71146|5|Briefly described|p6,  p43 fig 33|Middle Ordovician|Middle Ordovician|Amadeus Basin.||Larapinta Group||Unconformably overlies the Horn Valley Siltstone. Overlain by the Stokes Siltstone.|Sandstone.|
26147|Stairway Sandstone|71171|6|Mentioned|p2, p20|||Amadeus Basin. Coeval with the Goldwyer Formation. ||||||
26147|Stairway Sandstone|71279|5|Briefly described|p355 Fig.2, p365, p370, p374|Early Ordovician|Early Ordovician|Amadeus Basin. Has a K-radiometric high.||Larapinta Group.||||
26147|Stairway Sandstone|71342|6|Mentioned|Ch9 p16, Ch9 p20|||||||Unconformably overlies the Todd River Dolomite. Unconformably overlain by the Mereenie Sandstone.||
26147|Stairway Sandstone|71800|5|Briefly described|p26-p27|Middle Ordovician|Middle Ordovician|Amadeus Basin.||||Uncoformably overlies the Horn Valley Siltstone. Overlain by the Stokes Siltstone.|Quartz sandstone.|
26147|Stairway Sandstone|71898|5|Briefly described|p20|||Amadeus Basin.||||Unconformably overlies the Horn Valley Siltstone.||
26147|Stairway Sandstone|72360|5|Briefly described|Map legend|Ordovician|Ordovician|Of Amadeus Basin.||Unit of Larapinta Group.|||Sandstone, siltstone, limestone; marine fossils.|09-SEP-19
26147|Stairway Sandstone|72369|4|Described|iii,p3-4,29-31|||Of Amadeus Basin. Age constraint by fossils to Darriwilian (467-458 Ma) to early Gisbornian (460-456 Ma; Edgoose 2013 and references therein). Maidment (2005) provided a c. 465 Ma maximum depositional age, based on detrital zircon SHIRMP U-Pn analysis. LA-ICP-MS U-Pb detrital zircon dating of sample HB15ND556 (very fine- to fine-grained sandstone) yielded an interpreted maximum depositional age of 514+\-6 Ma (youngest concordant zircon), but does not further constrain the age of the formation as it is greater than the MDA provided by Maidment (2005). Contains zircons derived from the Musgrave Province (c. 1425-1045 Ma age spectrum). Neoproterozoic to Cambrian age zircon populations (c. 665-506 Ma or the c. 975-565 Ma) are inferred to have been derived from distal or buried sources.||Unit of Larapinta Group.||Overlain conformably by Stokes Siltstone. Underlain disconformably by Horn Valley Siltstone, or unconformably by Pertaoorrta Group.|Variably fossiliferous, commonly quartzic sandstone, with minor siltstone, limestone and phosphatic intervals.|
26147|Stairway Sandstone|73085|4|Described|piii, p1, p3-7, p11|early Ordovician|early Ordovician|Amadeus Basin. 21 m thick in drillhole LA05DD01. Top part of drillhole LA05DD01 are 'red beds' of this unit.||Larapinta Group||Underlain by Horn Valley Siltstone. Overlain by Stokes Siltstone.|Red-brown, fine-grained variably micaceous sandstone and lesser red-brown, finely laminated siltstone.|
26147|Stairway Sandstone|73119|5|Briefly described|piii, p1, p19-21, Appendix|Middle Ordovician (Darriwilian?)|Middle Ordovician (Darriwilian?)|Amadeus Basin, western. Broadly constrained by fossils. Geochron from Edgoose (2013). New SHRIMP U-Pb detrital zircon maximum deposition age of 578 +/- 7 Ma is probably older than the true depositional age; is older than previous age of 514 +/- 6 Ma (Normington et al., 2018). Detrital zircon age components are overwhelmingly dominated by a single Mesoproterozoic population at ca 1180 Ma suggesting that the bulk of detritus was likely derived from the Musgrave Province with negligible input from elsewhere. [See article for provenance discussion].|467-458 Ma|Larapinta Group||Conformably overlain by Stokes Siltstone.|Predominantly sandstone with lesser siltstone and limestone.|
26147|Stairway Sandstone|73279|5|Briefly described|p3, p11-12|Ordovician|Ordovician|Amadeus Basin. Middle part of the Larapinta Group. Detrital zircons analysed for Hf isotopic composition [see article].||Larapinta Group|||Includes sandstone.|
26147|Stairway Sandstone|73346|6|Mentioned|p10, p18-19|Late Ordovician|Early Ordovician|Amadeus Basin. Broadly similar in age to the Cobb Formation. Middle portion contains pelletal phosphorites. Includes the arandaspids Arandaspis prionotolepis, Porophoraspis crenulata, Porophoraspis sp., Arandaspis sp., and Sacabambaspis sp.||||||
34748|Stradbrooke Siltstone Member|22889|4|Described|p39|Adelaidean|Adelaidean|See p39 for location of type section and details of new stratigraphic unit. The Stradbrooke Siltstone Member superceds the former Stradbrooke Formation as the unit has been down graded from formation to member status, see p33 for details of change.||||||
35325|Strathearn Group|23345|5|Briefly described|43|||||||||
35325|Strathearn Group|23346|6|Mentioned|48|||||||||
35325|Strathearn Group|23347|2|Defined|p51 Tb. 1, p54|Calymmian|Statherian|Of the Willyama Supergroup. Comprises Mount Howden and Saltbush Subgroups. Age: ~1.69->1.48Ga. Overlies Curnamona Gp. Psammopelites + pelites, locally graphitic. Equiv. to Broken Hill, Sundown + Paragon Gps in Broken Hill Domain. Geol. prov: Olary Domain||||||24-FEB-10
35325|Strathearn Group|23476|5|Briefly described|p50 Fig 1|||||||||
35325|Strathearn Group|24289|5|Briefly described|p46, p47 Fig.2|Paleoproterozoic|Paleoproterozoic|Geological Province: Curnamona Province.||||||07-NOV-08
35325|Strathearn Group|24431|5|Briefly described|p189 Fig. 1|||Of the Willyama Supergroup. Overlies the Curnamona Group. Geological Province: Olary Domain.||||||
35325|Strathearn Group|60485|5|Briefly described|p28 Fig. 2|||Of the Willyama Supergroup.  Includes Mount Howden and Saltbush Subgroups, and the Plumbago Formation.  Geological Province: Olary Domain.||||||03-MAR-05
35325|Strathearn Group|61734|5|Briefly described|p52 Fig.2, p54-58, p68 Fig.9, p71|Statherian|Statherian|Mineral assemblages and fabrics associated with deformation are described.||Of the Willyama Supergroup.|Includes the Mount Howden and Saltbush Subgroups and Weekeroo Amphibolite.|Overlies the Curnamona Group.|Dominated by pelitic and minor psammitic rocks that contain varying amounts of graphite.|21-JUL-20
35325|Strathearn Group|61736|4|Described|p664, p666 Fig. 3|||Includes the Saltbush and Mount Howden Subgroups.Overlies Curnamona Group. Geological province: Olary Domain. See also p670, p671. See also Plumbago Formation.||||||24-FEB-10
35325|Strathearn Group|62373|5|Briefly described|p503|Paleoproterozoic|Paleoproterozoic|Of the Willyama Supergroup. Comprises Saltbush and Mount Howden Subgroups. Psammopelites and pelites. Geological Province: Curnamona Province/Olary Domain.||||||07-NOV-08
35325|Strathearn Group|62514|5|Briefly described|p748 Fig. 3|Mesoproterozoic|Mesoproterozoic|Includes Saltbush and Mount Howden Subgroups. Age: 1700-1650Ma. Geological Province: Olary Domain/Curnamona Province||||||16-SEP-09
35325|Strathearn Group|62535|5|Briefly described|p664, p666-668, p670-674|Paleoproterozoic|Paleoproterozoic|Maximum age of the lower part of the Group comes from the Plumbago Formation. Minimum age from Mooleulooloo Formation.|< c.1693 Ma to 1651 +/- 7 Ma.||Mooleulooloo Formation.|Overlies Curnamona Group.||
35325|Strathearn Group|62592|5|Briefly described|p14, p15, p16 Fig.2.2, p43.|||Olary Domain, Curnamona Province. Coeval with the northern Australian Pb-Zn basins; possibly prospective for Mount Isa and Century styles of mineralisation.  [presume age should be <1650 to >1640 Ma rather than as stated]|>1650 to <1640 Ma|Unit in Willyama Supergroup.|Includes Saltbush and Mount Howden Subgroups and Plumbago Formation.|Unconformably overlies Curnamona Group. Is intruded by Ninnerie Supersuite.||05-MAR-13
35325|Strathearn Group|62993|5|Briefly described|p13, p35, p37, p39, p42|Paleoproterozoic|Paleoproterozoic|Olary Domain.|||Includes Mount Howden Subgroup,|Overlies Walparuta Formation. Equivalent to Paragon Group.||19-DEC-21
35325|Strathearn Group|63102|5|Briefly described|p13-15,20,32,35-37,51-54,56-60,72|Statherian|Statherian|Geological province: Olary Domain, Curnamona Province. Widely distributed in Olary Domain, especially in the northern part of the outcropping region and bordering the Benagerie Ridge, however the top of Strathearn Group is not exposed or recognised anywhere. Of low grade metamorphic facies; quartz-muscovite-chlorite (+\-chloritoid) assemblage; also contains sillimanite and andalusite (sericite pseudomorphs). Contains stratiform mineralisation; small BIFs and Mc silicates.|c. 1685-1640 Ma||Includes Mooleulooloo Formation, Mount Howden Subgroup, Saltbush Subgroup, Plumbago Formation.|||22-OCT-19
35325|Strathearn Group|63186|5|Briefly described|p67, p67 Fig. 3, p70|Paleoproterozoic|Paleoproterozoic|Of the Mount Howden Subgroup (Willyama Supergroup). Includes Saltbush and Mount Howden Subgroups. Age: 1605+/-30Ma (garnet) and 1645 Ma. Geological Province: Broken Hill Domain, Curnamona Province.||||||07-NOV-08
35325|Strathearn Group|63539|5|Briefly described|p33|||Has contact with Curnamona Group. Geological Province: Olary Domain.||||||07-FEB-08
35325|Strathearn Group|63866|5|Briefly described|p41-p42|||Olary Domain, Curnamona Province. |1667-1640 Ma|Willyama Supergroup|Includes the Mooleulooloo Formation.|Overlies the Walparuta Formation.||
35325|Strathearn Group|64741|5|Briefly described|p301 Fig. 4|Paleoproterozoic|Paleoproterozoic|Of Willyama Supergroup. Includes Mount Howden Subgroup, Mooleulooloo and Dayana Formations. Geological province: Olary Domain, Curnamona province. Broadly equivalent to the Paragon Group in the Broken Hill Domain.||||||07-FEB-11
35325|Strathearn Group|64742|5|Briefly described|p320,  P323, p325, p330.|||Olary Domain. Major and trace element analyses, and Sm-Nd isotope data, are detailed.||Unit in Willyama Supergroup.|Includes Saltbush and Mount Howden Subgroups.|Overlies Curnamona Group.|Sequence of psammopelites and pelites.|29-MAR-12
35325|Strathearn Group|64944|5|Briefly described|p28 Fig. 1, p29 Tb. 1|Paleoproterozoic|Paleoproterozoic|Of the Willyama Supergroup. This group has been redefined to exclude Saltbush Group and includes Mount Howden Subgroup, Alconie, Mooleulooloo, Dayana Formations and undifferentiated upper level rocks. Age: 1670-1640Ma. Direct equivalent of Paragon Gp||||||07-FEB-11
35325|Strathearn Group|65407|6|Mentioned|p239 Fig.3||||||||Graphitic pyrite sediments, amphibolite, interbedded pelite and psammite.|
35325|Strathearn Group|66302|4|Described|p35, p36 Fig.9, p38, p39|Statherian|Statherian|Olary and Mulyungarie Domains, Curnamona Province. Represents sag phase deposition post-dating the climax of rifting.|1670-1640 Ma|Willyama Supergroup|Includes the Mount Howden Subgroup.|Equivalent to the Paragon Group.|Locally tuffaceous and includes aluminous mudstone, graphitic siltstone, albitic sandstone and brown mica schist.|
35325|Strathearn Group|67323|5|Briefly described|Eastern Australia Time-Space Plot; p35|Paleoproterozoic|Paleoproterozoic|Olary Domain, Curnamona Province. Post-rift sedimentation.|~1660-1650 Ma.||Dayana, Mooleulooloo, Alcoonie Formations.|||
35325|Strathearn Group|67536|5|Briefly described|Map Legend|Statherian|Statherian|Curnamona Province.|ca. 1693 +/- 3 Ma - 1648 +/- 6 Ma|Of the Willyama Supergroup.|||Psammopelite and pelite, locally graphitic; includes metasiltstone, Bumbarlow 1.|
35325|Strathearn Group|67540|6|Mentioned|p29 Tb.2|||||||||04-FEB-16
35325|Strathearn Group|67653|5|Briefly described|p4-5,11|||Geological province: Curnamona Province. ||Unit of Willyama Supergroup.||||
35325|Strathearn Group|68126|5|Briefly described|p6, p8, p15, p30|||Curnamona Province.|~1670-1640 Ma (Page et al. in prep).|Willyama Supergroup.||Equivalent to Paragon Group.|Psammopelite and pelite, locally graphitic.|
35325|Strathearn Group|69650|6|Mentioned|p6, p36|||||||||
35325|Strathearn Group|69654|6|Mentioned|p3|||Curnamona Province.||||||
35325|Strathearn Group|70405|5|Briefly described|p15, p25, p30, p43 Table 3, p96|Paleoproterozoic|Paleoproterozoic||1640 Ma - 1655 Ma|Wilyama Supergroup|Includes Mount Howden Subgroup||Dominated by pelitic metasediments with lesser metasandstone.|19-DEC-21
35325|Strathearn Group|70657|4|Described|p5, p6 Fig.1, p11 Fig.5, p12, p13 Fig.6|Statherian|Statherian|See also p14-17, p20, p24, p33, p40, p42-44, p57-58, p64-65, p77. Olary and Mulyungarie Domains, Curnamona Province. Conor (2000), for the upper part of the Willyama Supergroup in the Olary Domain; previously the Pelite Suite of Clarke et al. (1986). In this study, the Saltbush Subgroup is excised (and raised to Group rank). Lack of outcrop has hindered geological understanding. At least several hundred metres thick. Low-grade metamorphosed. Age also shown as ~1685 - 1640 Ma.|~1650 Ma.|Upper Willyama Supergroup|Mount Howden Subgroup.|Overlies Saltbush Group. Equivalent to the Paragon Group of Broken Hill Domain.||
35325|Strathearn Group|70658|5|Briefly described|p2, 15|Paleoproterozoic|Paleoproterozoic|Olary Domain, Curnamona Province. Represents sag-phase deposition.|~1655 Ma.|Willyama Supergroup.|Mount Howden Subgroup; Mooleulooloo Formation.|Overlies Saltbush Group. Equivalent to Paragon Group (Broken Hill Domain).||
35325|Strathearn Group|70858|6|Mentioned|p33|Paleoproterozoic|Paleoproterozoic|Olary Domain, Curnamona Province.||||||
35325|Strathearn Group|72454|6|Mentioned|p2 Fig.2, p8 Fig.6|Mesoproterozoic|Mesoproterozoic|Part of the Olary Domain. Shown only on p2 Fig.2 and p8 Fig.6.||Willyama Supergroup||||
35325|Strathearn Group|73429|5|Briefly described|p106 Fig.2, p107, p110, p111 Fig.6|Statherian|Statherian|Curnamona Province. Olary Domain, Mulyungarie Domain. Characterised by low magnetic response.||Willyama Supergroup, upper|Mount Howden Subgroup|Overlies Saltbush Group||
80217|Stud Dam Member|73162|5|Briefly described|p452, p453, p454, p458|Mesoproterozoic|Mesoproterozoic|Roopena Basin. Deposited in southeast part of the preserved basin. Records episode of extra-basinal felsic volcanism synchronous with sedimentation of Fresh Well Formation. Middle of three tuff members in the upper Fresh Well Formation. ~6m thick.||Fresh Well Formation, upper||Interlayered with the upper Fresh Well Formation.|Well sorted and laminated tuff, composed of quartz and minor lithic felsic volcanic and sedimentary clasts, matrix of sericite and clay, sharp basal and sharp to gradational upper contacts, approximately 6 m thick.|
29851|Stun Sail Boom Granite|64282|5|Briefly described|Map legend|Middle Cambrian|Middle Cambrian|Age: 505+/-7Ma(U-Pb). (Part of Delamerian Orogeny. Deformed, medium-gr., grey porphyritic quartz-plag.-biotite granite+opalescent blue qtz phenocrysts + large feldspar megacrysts. Xenoliths of recrystallised metasediment common, particularly in the ....||||||23-JUN-08
29851|Stun Sail Boom Granite|73107|5|Briefly described|Map legend.|Middle Cambrian|Middle Cambrian|Delamerian Orogeny.|505 +/- 7 Ma (U-Pb).||||Deformed, medium-grained, grey porphyritic quartz-plagioclase-biotite granite with opalescent blue quartz phenocrysts and large feldspar megacrysts. Xenoliths of recrystallised metasediment are common particularly in highly deformed marginal zones.|
79386|Sugarloaf Dam Sandstone|71037|5|Briefly described|p22-23 Fig.2, p29 Fig.9, p29|Neogene|Paleogene|Unconformably underlies undifferetiated Tertiary silcrete.||||Shown as younger than Tent Hill Formation.|Sandstone, well sorted, medium-grained, kaolinitic, with rhizomorphs, variably silicified.|
79386|Sugarloaf Dam Sandstone|71129|2|Defined|p3,137-141,145,148,150-151,210,225,229|Tertiary|Mesozoic|Geological Province: Gawler Craton. Type locality: Area extending for about 50 m around the point 741540mE, 6410005mN (GSA94, zone 53) 400 m NE to Sugarloaf Dam on Cariewerloo Station. Thickness at type section: 1-2m, maximum 5m. Reference drillhole: located around point 734333.5mE, 6412124.1mN (GSA94, zone 53) extending for about 50 m each way along a north-trending incised small gully, which eroded into the northern slope of a low hill. Outcrops  are restricted to the NE corner of SIX MILE HILL along foothills of the mesas in the vicinity of Cariewerloo Woolshed and along creek exposures between drill site MSDP02 and Martin Catch Dam. Deposited in a fluvial environment upon strong topographic relief; derived from reworking of weathered, matured sandstones or an aeolian sand source or aeolian reworking. Evidence of plant bioturbation rules out Neoproterozoic age.||||Underlain unconformably by Tregolana Shale Member or Simmens Quartzite Member.|Sandstone, well sorted, medium-grained, kaolinitic, with rhizomorphs, variably silicified; dominantly composed of subangular to rounded quartz grains in a kaolinitic matrix, with plant fragments.|13-NOV-19
79386|Sugarloaf Dam Sandstone|71131|5|Briefly described|Map legend.|||Age shown as Tertiary.|||||Well-sorted, medium-grained, kaolinitic sandstone, with rhizomorphs; variably silicified.|
79386|Sugarloaf Dam Sandstone|73234|2|Defined|p4-16, p18-23, App.|Miocene|Oligocene|New name [see ASUD for definition card]. Previously informally named on the Six Mile Hill 1:75,000 map sheet (Krapf et al., 2016; McAvaney et al., 2016) [this usage is indicated in the article as 'Sugarloaf Dam Sandstone']. Stuart Shelf. Occurs in the north-eastern corner of Six Mile Hill; exposed in dissected hilly terrain surrounding Cariewerloo Woolshed, about 25 km west-northwest of Port Augusta. Type locality: small hill located about 450 m northeast of Sugarloaf Dam on Cariewerloo Station. Reference locality: south-western foothills of South Tent Hill. Bedding structures: common massive appearance but variably distinct planar bedding structures. Grades laterally into a finer grained, friable to powdery, clay-rich material. Contains organosedimentary structures. Upper part is often variably indurated by silica (silcrete crust; named 'Corraberra surface' by Twidale et al., 1970). Unconformably overlain by coarse-grained, commonly gravelly sediments. Maximum thickness of 5 m but commonly 1 to 2 m. High compositional maturity but low textural maturity; thus interpreted as a sheet-like mass-flow deposit within an intermontane basin or sheltered embayment surrounded by the high tablelands. Age derived from relative timing of silcrete surfaces in the area. Detrital zircon signature dominated by late Mesoproterozoic grains and lacks zircons of the Hiltaba Suite-Gawler Range Volcanics event; did not contain any Phanerozoic zircons. Probably recycled from the Tent Hill Formation. Has implications for the Pirie and Torrens basins.||||Unconformably underlain by Tregolana Shale Member (Tent Hill Formation). Possibly equivalent to Neuroodla Formation.|White to light greenish grey or pale brown to pale red, moderately to well-sorted, fine- to medium-grained, rarely coarse-grained, kaolinitic sandstone with rare isolated cobble-sized well-rounded quartzite clasts.|
23998|Sullivan Shale Member|22629|6|Mentioned|p158|||||||||
23998|Sullivan Shale Member|23124|6|Mentioned|p397|||||||||
23998|Sullivan Shale Member|39905|5|Briefly described|p3|||||||||
23998|Sullivan Shale Member|41995|5|Briefly described|p12|||||||||
23998|Sullivan Shale Member|42465|5|Briefly described|Map Legend|||||||||
23998|Sullivan Shale Member|42469|4|Described|p14|||||||||
23998|Sullivan Shale Member|43052|4|Described|p69|||of Tarcoola Formation||||||
23998|Sullivan Shale Member|44935|5|Briefly described|Map Legend||Proterozoic|||||||
23998|Sullivan Shale Member|50605|5|Briefly described|p8.6|||Of the Tarcoola Formation. Geological Province: Gawler Craton & Curnamona Province.||||||
23998|Sullivan Shale Member|60704|5|Briefly described|p687, p688 Fig.2|Paleoproterozoic|Paleoproterozoic|Of the Tarcoola Formation. Age: 1656+/-7 Ma (U-Pb zircon). Carbonaceous, pyritic, micaceous, thin-bedded quartzite and siltstone (often referred to as "slates") interbedded with the Fabian Quartzite Member.||||||07-NOV-08
23998|Sullivan Shale Member|63276|5|Briefly described|p3 Fig. 2, p14 Fig. 3|Proterozoic|Proterozoic|Of the Tarcoola Formation. Thick sequence of thinly bedded carbonaceous, pyritic, micaceous quartzites and siltstones. See also p5 Fig. 4.||||||
23998|Sullivan Shale Member|64137|4|Described|p1543 Fig.2, p1544  |Paleoproterozoic|Paleoproterozoic|Depositional age; from tuffaceous units.|1657 +/- 7 Ma (U-Pb zircon; Daly, 1993).|Of the Tarcoola Formation.||Interbedded with Fabian Quartzite Member.|Carbonaceous, pyritic, micaceous, thin-bedded quartzites and siltstones.|
23998|Sullivan Shale Member|66302|6|Mentioned|p23, p32|Statherian|Statherian|Wilgena Domain, Gawler Craton. Deposited in a fluvial to marginal marine setting. Ages derived from water-lain tuffs.  |1657 +/- 11 Ma to 1654 +/- 3 Ma (Fanning, 1997)|Tarcoola Formation||Overlies the Fabian Quartzite Member.|Shale and water-lain tuffs.|
23998|Sullivan Shale Member|67058|5|Briefly described|p479, p491.|Paleoproterozoic|Paleoproterozoic|The tuff unit gives the age of this Member and the Tarcoola Formation.|1656 +/- 7 Ma (Daly 1993b).|Unit in Tarcoola Formation.|||Grey to black shales, interbedded with white quartzites of the Fabian Quartzite; includes a water-laid tuff.|
23998|Sullivan Shale Member|70778|6|Mentioned|p24|Statherian|Statherian|Central Gawler Craton. |1656 +/- 7 Ma (ID-TIMS)|Tarcoola Formation|||Dacitic to andesitic tuff.|05-SEP-19
82216|Sultan granite|72058|5|Briefly described|p175, 176, p184-185|Mesoarchean|Mesoarchean|Two samples analysed. Sample MB155 - pink granite Table 1, grey granite shown p176, pink altered granite Tables 2,3). Sample MB156 - grey granite Table 1, pink granite illustrated p176, leucogranite Tables 2,3. Rim growth at 2606+/-9 Ma may be a metamorphic overprint. Igneous crystallisation at 3238+/-9 Ma interpreted.  Major and trace element geochemistry discussed for both samples. See also page 174, Table 1, p181 Table 2.|3241+/-6 Ma, 3238+/-9 Ma.|||||16-MAR-21
27236|Summerfield Intrusive Suite|42884|2|Defined|p12|Early Ordovician|Late Cambrian|Supersedes Summerfield Granodiorite. See also Fig.2 p13.||||||26-MAR-08
31507|Swan Reach Dolomite Member|23179|6|Mentioned|Fig.2||Early Miocene|Mannum Formation, Murray Basin||||||
31507|Swan Reach Dolomite Member|23226|2|Defined|p896|Longfordian|Longfordian|Placed between the informal upper and lower Mannum Formation members. Of Mannum Formation.||||||
31507|Swan Reach Dolomite Member|63460|5|Briefly described|p845 Fig. 7|Early Miocene|Early Miocene|Within the upper Mannum Formation. Geological province: Murray Basin.||||||
31507|Swan Reach Dolomite Member|64237|5|Briefly described|p19 Fig. 2b|Middle Miocene|Early Miocene|Of the Mannum Formation (Murray Group). Originally introduced as a new member with the stratigraphic revision of the Murray Group up to Murray Supergroup by Lukasic and James (1998), but retained when Murray Group was reinstated.||||||
24005|Symons Granite|22629|5|Briefly described|fig2p147,158|Statherian|Statherian|Age: 1690+/-10Ma||||||
24005|Symons Granite|24197|5|Briefly described|p74 Tb. 8.1|Paleoproterozoic|Paleoproterozoic|Age: 1750-1700Ma.||||||07-FEB-11
24005|Symons Granite|39802|6|Mentioned|Map legend|Proterozoic|Proterozoic|Post-Kimban Orogeny||||||
24005|Symons Granite|40644|6|Mentioned|p124 Fig. 3, p133|Mesoproterozoic|Paleoproterozoic|Included in the Lincoln Complex grouping. Age: 1585+/-12Ma (Rb-Sr) - see p133 Fig. 22. Age: ca. 1675Ma also presented (p133).||||||02-JUN-09
24005|Symons Granite|43052|5|Briefly described|Table 4.4|||of ?Lincoln Complex||||||
24005|Symons Granite|44935|5|Briefly described|Map Legend||Proterozoic|||||||
24005|Symons Granite|50605|5|Briefly described|p(i), 1.3, 5.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Gawler Craton and Curnamona Province. Age: 1700-1680Ma (U-Pb). Of the Younger Lincoln Supersuite.||||||07-NOV-08
24005|Symons Granite|60484|5|Briefly described|p36|||At Mulgathing Rocks.  Coarse-grained, foliated, porphyritic pink granite and augen gneiss with large microcline crystals.  Intrudes the Archaean  Mulgathing Complex. Age: 1684+/-10Ma. Time equivalent of the Tunkillia Suite.||||||03-MAR-05
24005|Symons Granite|60953|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Gneissic granite and adamellite.||||||07-NOV-08
24005|Symons Granite|61108|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|Gneissic granite and adamellite. Age: 1702-1690 Ma.||||||07-NOV-08
24005|Symons Granite|63067|5|Briefly described|p2 Fig. 1|Paleoproterozoic|Paleoproterozoic|Age: ~1690Ma.||||||07-NOV-08
24005|Symons Granite|64137|6|Mentioned|p1553 Fig.8 |||Neodymium isotope data.||||||
24005|Symons Granite|65375|6|Mentioned|p13.|Paleoproterozoic|Paleoproterozoic||1684 Ma.|||||
24005|Symons Granite|65376|5|Briefly described|p178 Fig.5.26, pp207-210.|Paleoproterozoic|Paleoproterozoic|Forms a homogeneous, foliated granitic batholith of considerable size.|1686 +/- 10 Ma.||||Pink, foliated granite containing abundant quartz, coarse K-feldspar and a low percentage of plagioclase and biotite.|
24005|Symons Granite|65385|6|Mentioned|pS128 Fig. 2|Statherian|Statherian|1686 +/-10 Ma.||||||08-MAR-12
24005|Symons Granite|65390|6|Mentioned|p21, p22 Fig. 3|Statherian|Statherian|Wilgena Domain, Gawler Craton. Immediately W of Mulgathing Homestead. Age 1690 +/- 10 Ma.||||||
24005|Symons Granite|65922|6|Mentioned|p9|Statherian|Statherian|Of Ifould Complex. ~1685-1670 Ma.||||||
24005|Symons Granite|66302|6|Mentioned|p23, p24|Statherian|Statherian||1686 +/- 10 Ma (SHRIMP U-Pb, Fanning et al, 2007)|Tunkillia Suite||||
24005|Symons Granite|67117|6|Mentioned|Map legend.|||Shown in Solid Geology Interpretation 1:1M figure as '?Engenina Adamellite, Symons Granite, equivalents of Tunkilla Suite'.||||||03-MAY-13
24005|Symons Granite|67536|5|Briefly described|Map Legend|Statherian|Statherian|Gawler Craton. Mapped (LM14) with several units of deformed gabbro and granite of the Kararan Orogeny and earlier transitional Kimban-Kararan events.|1690 +/- 10 Ma.||||Part of a collection of deformed gabbro to granite of the Kararan Orogeny and earlier transitional Kimban-Kararan events.|02-APR-14
24005|Symons Granite|72459|5|Briefly described|p22, p51|Palaeoproterozoic|Palaeoproterozoic|Wilgena Subdomain of the Gawler Craton. Interpreted to be of the Ifould Magmatic event.|1684 +/- 10 Ma|||||
24005|Symons Granite|73112|5|Briefly described|Map legend.|||Shown in the Solid Geology Interpretation map, below the main Nullarbor 250k map. The Engenina Adamellite, Symons Granite, equivalents of Tunkillia Suite are all mapped as one unit.||||||
24005|Symons Granite|73235|6|Mentioned|p53|Statherian|Statherian|Gawler Craton. Wilgena and Harris Greenstone regions.|1685 Ma|||||
24005|Symons Granite|73298|6|Mentioned|p1077 Tb.2|Statherian|Statherian|Gawler Craton.|1684 +/- 10 Ma|||||
33821|Taloola Ignimbrite Member|63056|5|Briefly described|p81 Fig. 2|Early Cambrian|Early Cambrian|Of the Mooracoochie Volcanics. Thickness: >78m. Geological. Province: Warburton Basin.||||||07-FEB-08
33821|Taloola Ignimbrite Member|65489|5|Briefly described|p120|Early Cambrian|Early Cambrian|Eastern Warburton Basin.||Unit in Mooracoochie Volcanics.||||
33821|Taloola Ignimbrite Member|68731|6|Mentioned|p170 Fig 3.83|Early Cambrian|Early Cambrian|> 78 m thick.||||||
33821|Taloola Ignimbrite Member|69982|3|Fully described|p15,p17-19,p21, p44, p51, p56, p162-164|Early Cambrian|Early Cambrian|See also Appendix 1. New name. Type section is the interval 1940.1 - 2018 m in Sturt 7 well. Distinguished as a separate Member because of the significance of the ignimbrites as a potential reservoir. Mis-spelt as Talloola on p19; rank is omitted on p66, p69, p71, p86, p106. Reservoir attributes described. Produces oil in Sturt 6 well. Brief thin section descriptions. Composite logs shown.||Unit in Mooracoochie Volcanics.|||Orange to brown, coarse-grained, crystal and shard-rich ignimbrite, varying from massive (non-welded) to planar-foliated (welded).|
22945|Tanana Formation|22746|4|Described|Fig.3 p515, p521|Neoproterozoic III|Neoproterozoic III|||||||
22945|Tanana Formation|22802|6|Mentioned|p872|||Officer Basin.||||||30-SEP-08
22945|Tanana Formation|22921|6|Mentioned|39|||Geol province Officer Basin.||||||30-SEP-08
22945|Tanana Formation|22922|5|Briefly described|34|||Parent Ungoolya Group||||||
22945|Tanana Formation|23282|2|Defined|p62||Neoproterozoic|Defined by Zang (1995), previously termed upper 'Ungoolya Formation' (Dunster 1987) and upper Rodda beds (Brewer etal 1987, Stainton etal 1988). Age: Precambrian, Neoproterozoic, mid Marinoan Epoch. of Ungoolya Gp.||||||
22945|Tanana Formation|23524|5|Briefly described|p221 Fig. 3|Neoproterozoic|Neoproterozoic|||||||
22945|Tanana Formation|24112|5|Briefly described|p254 Fig.2, p257 Tb.1|Neoproterozoic|Neoproterozoic|Of the Ungoolya Group. Age: 585-575Ma. Geological Province: Officer Basin||||||
22945|Tanana Formation|43622|6|Mentioned|p39|||||||||
22945|Tanana Formation|43743|6|Mentioned|Fig.2,p33||Neoproterozoic|||||||
22945|Tanana Formation|50127|6|Mentioned|p48 Fig.2|||Geological Province: Officer Basin.||||||30-SEP-08
22945|Tanana Formation|61732|3|Fully described|p5 Tb. 1, p62-64|Marinoan|Marinoan|Of Ungoolya Gp; previously referred to as "upper Ungoolya Fm" and "upper Rodda beds". Overlies Karlaya Lmst. Conformably overlain by Muyarai Fm. Unconformably overlain by Narana Fm. Geol.Prov: Officer Basin. See p58 Fig. 22.||||||07-FEB-11
22945|Tanana Formation|62085|6|Mentioned|p15 Fig.1|||Officer Basin. Contains acritarch: Tanarium conoideum.||||||
22945|Tanana Formation|63397|2|Defined|29-30|Neoproterozoic III|Neoproterozoic III|Of the Ungoolya Group. Type section in text. Limestone, calcareous siltstone and minor sandstone. Thickness: 521m. Conformably overlies Dey-Dey Mudstone. Overlain by Narana Formation and Munyarai Formation.||||||18-JUL-07
22945|Tanana Formation|63811|5|Briefly described|p500, 502, Fig 2, p519-528 App A|Ediacaran|Ediacaran|Contains acritach species. Correlated with Siberian, Russian and Chinese units.||||Overlies the Karlaya Limestone, of the Ungoolya Group.|Micritic limestone with silty mudstone interbeds of prodelta, distal delta and shelf environments.|28-MAR-12
22945|Tanana Formation|64794|4|Described|p251, p254-266, p269-270, p272-276|Ediacaran|Ediacaran|See also p238 fig 2, p240 Tb.1, p242 fig 3, p245-8. 462m thick at Munta 1. Lithology described in some detail in Tb.1. Upper part underwent canyon-forming erosion. Organic content and biomarkers treated in great detail.||Ungoolya Group||Overlies Karlaya Limestone. Is unconformably overlain by Narana Formation.|Intercalated succession of (a) marly mudrock intervals with siltstone and minor fine sandstone with (b) micritic limestone with thin interbeds of siltstone or marl.|
22945|Tanana Formation|64797|6|Mentioned|p153 Fig.2|Ediacaran|Ediacaran|Officer Basin. Lithology/rank not shown on diagram.||||||
22945|Tanana Formation|66569|5|Briefly described|p861 fig.2,|Ediacaran|Ediacaran|Of Ungoolya Group; unconformably underlies Munyarai Formation; overlies Karlaya Limestone.||||||
22945|Tanana Formation|67620|6|Mentioned|p22|||Officer Basin. Contains abundant organic laminae (microbial mats).||||||
22945|Tanana Formation|67912|6|Mentioned|p13|Ediacaran|Ediacaran|Eastern Officer Basin. Subsurface.||Ungoolya Group.|Wilari Dolomite Member.|||
22945|Tanana Formation|68269|6|Mentioned|p674|Ediacaran|Ediacaran|Officer Basin.||Ungoolya Group||Underlain by Karlaya Limestone. Unconformably overlain by Munyarai Formation.|Mudstone dominated.|
22945|Tanana Formation|72478|6|Mentioned|p8|Marinoan|Neoproterozoic|Officer Basin. Age described as Marinoan.|c. 585 Ma|Ungoolya Group|Includes the Wilari Dolomite Member|Overlies the Karlaya Limestone. Unconformabnly overlain by the Narana Formation. Overlain by the Munyarai Formation.||24-MAR-21
22945|Tanana Formation|73099|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Officer Basin.||Ungoolya Group.|Wilari Dolomite Member.|Overlies Karlaya Limestone. Is overlain by Narana Formation.|Grey to medium brown, laminated to thin-bedded siltstone, calcareous and dolomitic in part, and interbeds of very fine-grained sandstone to intraformational conglomerate.|
22945|Tanana Formation|73392|6|Mentioned|p3||||||||Sampled from core of Giles 1 well.|
26161|Tandanya Sand Member|22541|6|Mentioned|p29|||Chinaman Gully Formation||||||
26161|Tandanya Sand Member|35542|2|Defined|p2|middle Tertiary|middle Tertiary|Part of Chinaman Gully Formation.||||||
26161|Tandanya Sand Member|36244|6|Mentioned|p2|||Defined by Lindsay & Harris 1979.||||||
26161|Tandanya Sand Member|37324|6|Mentioned|p11|||||||||
26161|Tandanya Sand Member|38107|6|Mentioned|Table 1|||||||||
26161|Tandanya Sand Member|40453|6|Mentioned|Fig.2|||||||||
26161|Tandanya Sand Member|41025|6|Mentioned|Fig.2|||||||||
26161|Tandanya Sand Member|41513|6|Mentioned|p42|||||||||
26161|Tandanya Sand Member|41520|4|Described|Fig.5|||||||||
26161|Tandanya Sand Member|42574|6|Mentioned|Fig.2 P242|||||||||
26161|Tandanya Sand Member|42733|5|Briefly described|map legend|Tertiary||||||||
26161|Tandanya Sand Member|44133|5|Briefly described|p165 Fig. 10.11, 168|Late Eocene|Late Eocene|Geological Province: Saint Vincent Basin. Of the Chinaman Gully Formation. ||||||
26161|Tandanya Sand Member|70660|6|Mentioned|p18|||||Chinaman Gully Formation||||
26926|Tapanappa Formation|22458|4|Described|p524||Cambrian|Of Kanmantoo Group.||||||27-MAY-08
26926|Tapanappa Formation|22573|6|Mentioned|p 53|||||||||
26926|Tapanappa Formation|22643|5|Briefly described|p186, fig3,6,7|Early Cambrian|Early Cambrian|||||||
26926|Tapanappa Formation|22840|6|Mentioned|Table1 P38|||||||||
26926|Tapanappa Formation|23317|5|Briefly described|380 Fig.2|||||||||
26926|Tapanappa Formation|23539|5|Briefly described|Fig 1 p 467|||||||||
26926|Tapanappa Formation|23731|5|Briefly described|p17, p27|Cambrian|Cambrian|||||||
26926|Tapanappa Formation|23981|5|Briefly described|p13|Early Cambrian|Early Cambrian|Of the Kanmantoo Group. Geological Province: Stansbury Basin (Fleurieu Peninsula).||||||
26926|Tapanappa Formation|23996|5|Briefly described|p352 Fig.1|Cambrian|Cambrian|Of Kanmantoo Group.  Geological Province: Adelaid Fold Belt.||||||07-MAR-05
26926|Tapanappa Formation|24381|5|Briefly described|p58|||Of Kanmantoo Group.||||||
26926|Tapanappa Formation|24465|4|Described|p355|Early Cambrian|Early Cambrian|Overlies Talisker Formation. Of Bollaparudda Subgroup (Kanmantoo Group). Dyson et al (1996) included unit in their Silverton Subgroup. Approx. 3000m thick at type section.||||||19-JAN-05
26926|Tapanappa Formation|30377|3|Fully described|p206|||||||||
26926|Tapanappa Formation|30378|6|Mentioned|p431|||||||||
26926|Tapanappa Formation|30380|6|Mentioned|Table 1|||Correlation||||||
26926|Tapanappa Formation|30381|4|Described|p215|||See also P216||||||
26926|Tapanappa Formation|35089|6|Mentioned|p219|||||||||
26926|Tapanappa Formation|35255|6|Mentioned|Fig.8|||||||||
26926|Tapanappa Formation|36836|6|Mentioned|Table 1|||||||||
26926|Tapanappa Formation|38699|6|Mentioned|p16|||||||||
26926|Tapanappa Formation|38873|4|Described|Table 2|||||||||
26926|Tapanappa Formation|38927|6|Mentioned|p45|||||||||
26926|Tapanappa Formation|39350|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
26926|Tapanappa Formation|40196|6|Mentioned|p1826|||||||||
26926|Tapanappa Formation|40228|5|Briefly described|p39|||||||||
26926|Tapanappa Formation|40442|6|Mentioned|Table 1|||||||||
26926|Tapanappa Formation|40454|6|Mentioned|p46|||||||||
26926|Tapanappa Formation|40455|5|Briefly described|p71|||||||||
26926|Tapanappa Formation|40856|6|Mentioned|Fig.23.6|||||||||
26926|Tapanappa Formation|41253|6|Mentioned|p57|||||||||
26926|Tapanappa Formation|41947|6|Mentioned|p16|||||||||
26926|Tapanappa Formation|42225|6|Mentioned|Fig.4 P224|||||||||
26926|Tapanappa Formation|42243|5|Briefly described|p211|||||||||
26926|Tapanappa Formation|42270|6|Mentioned|p353|||||||||
26926|Tapanappa Formation|42271|6|Mentioned|Fig.5 P376|||||||||
26926|Tapanappa Formation|42499|5|Briefly described|Map legend|Cambrian||||||||
26926|Tapanappa Formation|42505|5|Briefly described|Map legend|Cambrian||||||||
26926|Tapanappa Formation|43703|6|Mentioned|p75|||||||||
26926|Tapanappa Formation|43759|6|Mentioned|p445|||||||||
26926|Tapanappa Formation|44133|5|Briefly described|p4 Fig. 7.2, 15, 17, 18|Early Cambrian|Early Cambrian|Geological Province: Stansbury Basin. Of the Kanmantoo Group.  Overlain conformably by the Tunkalilla Formation.||||||
26926|Tapanappa Formation|60712|4|Described|p35-36, p28 Fig. 1, p30 Fig. 3|Early Cambrian|Early Cambrian|Of the Silverton Subgroup. Medium to dark grey, thick-bedded to laminated, generally fine- to coarse-grained metasandstone; outcrops of small-scale, lenticular conglomerate beds.........Overlies Talisker Calc-siltstone. Type section inc.||||||
26926|Tapanappa Formation|61046|5|Briefly described|p7, p8 Fig.2, p9-11|Early Cambrian|Early Cambrian|Of Kanmantoo Group. Metagreywacke with metasiltstone interbeds and pyritic schist units. Also micaschist+/-andalusite, garnet, staurolite, and BIF in some areas. Hosts mineralisation: Cu-Au in garnet-andalusite-biotite schist; Zn-Pb-Ag in turbidites.||||||
26926|Tapanappa Formation|61237|5|Briefly described|p36|Cambrian|Cambrian|East of Adelaide this unit contains a horizon now quarried for bluestone - the Kanmantoo and Wistow Bluestones. Now extensively used for walling and paving stone.||||||27-MAY-06
26926|Tapanappa Formation|61307|5|Briefly described|p6 Fig. 3, p25|Cambrian|Cambrian|Of Carrickalinga Head Formation (Kanmantoo Group). Classic andalusite-garnet-staurolite schists in the Kanmantoo area. Geological Province: Adelaide Fold Belt.||||||
26926|Tapanappa Formation|61838|6|Mentioned|p221|||With associated ferruginous saprolites.||||||
26926|Tapanappa Formation|63848|6|Mentioned|p531,  p534 Fig.4.|||Southern Fleurieu Peninsula. Possibly contains poorly preserved trilobites.||Unit in Kanmantoo Group.||Overlies Talisker Formation. Is overlain by Tunkalilla Formation.||02-MAY-12
26926|Tapanappa Formation|65375|5|Briefly described|p33.|Early Cambrian|Early Cambrian|||Unit in Kanmantoo Group.||Overlies Talisker Formation. Is overlain by Tunkalilla Formation.||
26926|Tapanappa Formation|65664|5|Briefly described|p1096, p1100,  p1101-6, Tabs.1-4, Fig.5|Early Cambrian|Early Cambrian|Deposited in a shallow water turbiditic environment.||Of Bollaparudda Subgroup.||Overlies Talisker Formation. Overlain by Tunkalilla Formation.||09-MAY-12
26926|Tapanappa Formation|65892|5|Briefly described|p9 Fig.4. |Middle Cambrian|Early Cambrian|Fleurieu Peninsula.||Unit in Kanmantoo Group.||Overlies Talisker Formation. Is overlain by Tunkalilla Formation.||
26926|Tapanappa Formation|65921|5|Briefly described|p1, p2 (map legend).|Cambrian|Cambrian|Occurs as a shore platform north of the town of Penneshaw. Considered to be a deep water equivalent to the White Point Conglomerate at Bald Rock.||Of the Kanmantoo Group.|||Sandstone containing a number of channelised pebble beds with granite, gneiss, quartzite and limestone clasts.|
26926|Tapanappa Formation|68735|6|Mentioned|p235 Fig.3|Early Cambrian|Early Cambrian|Fleurieu Peninsula.||Of the Kanmantoo Group.||||10-APR-17
26926|Tapanappa Formation|68993|6|Mentioned|p544 Fig.1|Early Cambrian|Early Cambrian|Fleurieu Peninsula.||Of the Kanmantoo Group.||||
26926|Tapanappa Formation|71593|6|Mentioned|p150|||Hosts Cu and Au mineralisation.||||||
26926|Tapanappa Formation|73093|5|Briefly described|map legend|Cambrian|Cambrian||||||Sandstone to greywacke, fine to coarse-grained, dark grey, thick-bedded to laminated; interbedded with laminated siltstone and thin, sulphidic siltstone and lenticular grit to conglomerate beds.|09-DEC-21
26926|Tapanappa Formation|73107|5|Briefly described|Map legend.|Early Cambrian|Early Cambrian|Kanmantoo Trough.||Kanmantoo Group.|||Grey, massive and convoluted fine to coarse-grained metasandstone. Trough and tabular crossbeds with low angle foresets. Erosional bases with cut-and-fill structures grading up into laminated siltstone interbeds.|
26926|Tapanappa Formation|73188|6|Mentioned|p316|Early Cambrian|Early Cambrian|Mount Lofty Ranges.||Bollaparudda Subgroup, Kanmantoo Group|||Medium-grained turbidites.|
34724|Taratap Granodiorite|22848|2|Defined|35|Pridoli|Tremadoc|Age 475+/- 65 Ma||||||01-APR-14
34724|Taratap Granodiorite|73093|5|Briefly described|map legend|Ordovician|Cambrian||||||Granodiorite, blue-grey, porphyritic, hornblende-biotite. Comagmatic and metasedimentary enclaves. S-type, post-tectonic.|09-DEC-21
27907|Tarcowie Siltstone|22510|5|Briefly described|table1p37,41|||Of the Upalinna Subgroup.  Age: Marinoan. Mid-North Region.||||||13-OCT-04
27907|Tarcowie Siltstone|22631|6|Mentioned|p178|||Age: Marianoan||||||
27907|Tarcowie Siltstone|22772|5|Briefly described|Table13.1|Neoproterozoic III|Neoproterozoic III|||||||
27907|Tarcowie Siltstone|22857|5|Briefly described|Tb. 13.1 (insert p70-71)|Marinoan|Marinoan|Of the Farina Subgroup (Umberatana Group). Age: <610Ma.||||||
27907|Tarcowie Siltstone|22926|6|Mentioned|39 fig 2|Neoproterozoic|Neoproterozoic|Geol province Adelaide Geosyncline. Parent Umberatana Group||||||
27907|Tarcowie Siltstone|23314|5|Briefly described|331 Fig.2|||||||||
27907|Tarcowie Siltstone|23818|4|Described|p64 Fig.22, p69|Neoproterozoic|Neoproterozoic|Of the Amberoona Formation. Max. thickness: ~3000 ft. Overlain by Enorama Shale.||||||19-FEB-08
27907|Tarcowie Siltstone|24364|6|Mentioned|p29 Fig.3|Neoproterozoic|Neoproterozoic|||||||
27907|Tarcowie Siltstone|24584|5|Briefly described|p14 Fig. 2|Neoproterozoic|Neoproterozoic|Sandy siltstone.||||||
27907|Tarcowie Siltstone|29778|6|Mentioned|p167|||||||||
27907|Tarcowie Siltstone|29780|4|Described|p38|||||||||
27907|Tarcowie Siltstone|29837|4|Described|p61|||||||||
27907|Tarcowie Siltstone|30052|6|Mentioned|Fig.6|||Proterozoic age.||||||
27907|Tarcowie Siltstone|30053|6|Mentioned|p113|||||||||
27907|Tarcowie Siltstone|30261|6|Mentioned|Table 1|||Marinoan age||||||
27907|Tarcowie Siltstone|30801|6|Mentioned|p5|||Table p5-6.||||||19-FEB-08
27907|Tarcowie Siltstone|30805|6|Mentioned|p1|||||||||
27907|Tarcowie Siltstone|30807|6|Mentioned|p103|||Suggested map symbol||||||
27907|Tarcowie Siltstone|31538|6|Mentioned|p172|||See also Fig. 1||||||
27907|Tarcowie Siltstone|32146|6|Mentioned|Fig.3|||||||||
27907|Tarcowie Siltstone|32481|6|Mentioned|Fig.10|||Stratigraphy on P21||||||
27907|Tarcowie Siltstone|32724|6|Mentioned|Fig.1|||Marinoan. Correlation||||||
27907|Tarcowie Siltstone|33474|6|Mentioned|Fig.2|||||||||
27907|Tarcowie Siltstone|34535|5|Briefly described|p69|||See Fig.22||||||
27907|Tarcowie Siltstone|34536|6|Mentioned|Map legend|Adelaidean|Adelaidean|Farina Sub-Gp.Marinoan||||||
27907|Tarcowie Siltstone|36733|6|Mentioned|Table 5|||||||||
27907|Tarcowie Siltstone|37461|6|Mentioned|Table 5.I|||See also P341||||||
27907|Tarcowie Siltstone|38110|6|Mentioned|p2|||||||||
27907|Tarcowie Siltstone|38157|6|Mentioned|Table IV|||||||||
27907|Tarcowie Siltstone|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Marinoan||||||
27907|Tarcowie Siltstone|39348|6|Mentioned|Map legend|Adelaidean|Adelaidean|Marinoan||||||
27907|Tarcowie Siltstone|39350|6|Mentioned|Map legend|Precambrian|Precambrian|Sturtian||||||
27907|Tarcowie Siltstone|40294|5|Briefly described|p51|||||||||
27907|Tarcowie Siltstone|40442|6|Mentioned|p10|||||||||
27907|Tarcowie Siltstone|41405|3|Fully described|p175|||||||||
27907|Tarcowie Siltstone|41494|6|Mentioned|Fig.2|||||||||
27907|Tarcowie Siltstone|41500|4|Described|p80|||||||||
27907|Tarcowie Siltstone|41526|6|Mentioned|p5|||||||||
27907|Tarcowie Siltstone|42098|5|Briefly described|p54|||||||||
27907|Tarcowie Siltstone|42109|5|Briefly described|p18|||||||||
27907|Tarcowie Siltstone|42222|6|Mentioned|p17|||||||||
27907|Tarcowie Siltstone|42239|6|Mentioned|p161|||||||||
27907|Tarcowie Siltstone|42505|5|Briefly described|Map legend|Adelaidean (Marinoan)||||||||
27907|Tarcowie Siltstone|42542|5|Briefly described|Fig.2a P11|||||||||
27907|Tarcowie Siltstone|42720|5|Briefly described|map legend|Marinoan||||||||
27907|Tarcowie Siltstone|42813|5|Briefly described|p20|||Of Farina Subgroup.||||||19-FEB-08
27907|Tarcowie Siltstone|42882|4|Described|p10, Fig.5 p8|||Of the Umberatana Group.||||||19-FEB-08
27907|Tarcowie Siltstone|43052|5|Briefly described|p189,Table 6.1|||Of Farina Subgroup.||||||19-FEB-08
27907|Tarcowie Siltstone|43742|6|Mentioned|Fig.2,p39||Neoproterozoic|||||||
27907|Tarcowie Siltstone|43845|5|Briefly described|Fig3 p43||Neoproterozoic|In Umberatana Group||||||12-JUL-16
27907|Tarcowie Siltstone|44690|4|Described|map legend|||Geol. Atlas Series. (I/54-5). Marinoan.||||||
27907|Tarcowie Siltstone|60959|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Of the Upalinna Subgroup. Grey-green siltstone with laminations of brown sandy siltstone, fine sandstone and thin grey shale. Medium grained sandstone and grit at base.||||||11-MAY-05
27907|Tarcowie Siltstone|61732|5|Briefly described|p28 Fig. 13|Marinoan|Marinoan|Of the Upalinna Subgroup (Umberatana Group). Geological Province: Adelaide Rift Complex.||||||07-FEB-11
27907|Tarcowie Siltstone|64282|5|Briefly described|Map legend|Neoproterozoic III|Neoproterozoic III|Geological Province: Adelaide Geosyncline. Grey, flaggy, sandy siltstone and thin sandstone.||||||01-JUL-08
27907|Tarcowie Siltstone|65925|5|Briefly described|Appendix 2.||||||||Siltstone, sandy, flaser bedded.|
27907|Tarcowie Siltstone|67030|6|Mentioned|p409 Fig. 2|Cryogenian|Cryogenian|Shown as lateral equivalent to Angepena Formation||Farina Subgroup||Overlies the Tapley Hill Formation and ?Cox Sandstone; underlies the Waukaringa Siltstone.||26-APR-12
27907|Tarcowie Siltstone|70334|5|Briefly described|p90|Neoproterozoic|Neoproterozoic|Geological province: Gawler Craton. Of Adelaide Geosyncline and Stuart Shelf. Contains structurally controlled quartz-carbonate veins and stock work zones with potential to host Au mineralisation.||Unit of Umberatana Group.|Includes Cox Sandstone Member.|||
27907|Tarcowie Siltstone|70407|5|Briefly described|p103 Fig 2|Neoproterozoic|Neoproterozoic|Age: Marinoan.||Of Umberatana Group.||Basal unconformity, over Tapley Hill Formation.||
27907|Tarcowie Siltstone|71237|14|Not recorded|p9, 18|||||||||
27907|Tarcowie Siltstone|73107|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Adelaide Geosyncline.|||||Grey flaggy sandy siltstone and thin sandstone.|
27907|Tarcowie Siltstone|74367|6|Mentioned|p7 Fig.6|||||||||
22952|Tarella Silt|44133|5|Briefly described|p164, 152 Fig. 10.2|Oligocene|Oligocene|Geological Province: Saint Vincent Basin. Thickness: 20m. ||||||
22953|Tarlina Sandstone|22746|4|Described|Fig.3 p515, p519|Neoproterozoic III|Neoproterozoic III|||||||
22953|Tarlina Sandstone|22922|5|Briefly described|34|||Parent Lake Maurice Group||||||
22953|Tarlina Sandstone|23282|2|Defined|p56||Neoproterozoic|Age: Precambrian, Neoproterozoic, early Marinoan Epoch. was Tarlina beds of Stainton 1988, changed informally by Sukanta 1993 and formalised by Zang 1995.||||||
22953|Tarlina Sandstone|23286|6|Mentioned|p89|||||||||
22953|Tarlina Sandstone|23287|6|Mentioned|Fig.2,4|||Age: Lower Ediacarian. of Eastern Officer Basin.||||||
22953|Tarlina Sandstone|23288|6|Mentioned|p128 Fig.5|||||||||
22953|Tarlina Sandstone|23524|5|Briefly described|p221 Fig. 3|Neoproterozoic|Neoproterozoic|||||||
22953|Tarlina Sandstone|24112|5|Briefly described|p254 Fig.2, p257 Tb.1|Neoproterozoic|Neoproterozoic|Of the Lake Maurice Group. Age: 650-640Ma. Geological Province: Officer Basin||||||
22953|Tarlina Sandstone|43657|6|Mentioned|Fig.3,p4||Neoproterozoic|||||||
22953|Tarlina Sandstone|43690|6|Mentioned|Fig.2,p157||Neoproterozoic|||||||
22953|Tarlina Sandstone|43743|6|Mentioned|Fig.2,p33||Neoproterozoic|||||||
22953|Tarlina Sandstone|44109|5|Briefly described|p22 Fig. 19|Neoproterozoic|Neoproterozoic|Geological Province: central Officer Basin.||||||
22953|Tarlina Sandstone|61732|5|Briefly described|p57 Fig. 21, p58 Fig. 22|Cryogenian|Cryogenian|Of the Lake Maurice Group. Overlain by Murnaroo Formation. Geological Province: southeastern Officer Basin. See also p145 Fig. 51.||||||07-FEB-11
22953|Tarlina Sandstone|63397|2|Defined|26-27|Neoproterozoic III|Neoproterozoic III|Of the Maurice Group. Type section in text. Predominantly sandstone with minor thin silty mudstone interbeds. Thickness: 169m. Unconformably overlies the Alinya Formation. Conformably overlain by Meramangye Formation.||||||18-JUL-07
22953|Tarlina Sandstone|64794|5|Briefly described|p238 fig 2|Ediacaran|Ediacaran|Mis-named as Tarlina Formation on p244.|650 Ma basal age.|Lake Maurice Group|||Coarse marine and non-marine clastics.|
22953|Tarlina Sandstone|64796|6|Mentioned|p200 Fig.10|Neoproterozoic|Neoproterozoic|Appears in Fig.10 without the lithology.||||||
22953|Tarlina Sandstone|66569|5|Briefly described|p861 fig.2,|||Unconformably underlies Meramangye Formation.||||||
22953|Tarlina Sandstone|68269|6|Mentioned|p674|||||||Unconformably overlain by Meramangye Formation.|Sandstone dominated.|
22953|Tarlina Sandstone|69648|4|Described|p17-19, p34, map legend|Neoproterozoic|Neoproterozoic|Lowstand. Age: Marinoan. Probable equivalents of this unit have been interpreted from drillhole logs. Correlated in drillholes on OOLDEA.||Lake Maurice Group||Unconformably (although structurally conformable) overlies Alinya Formation (major hiatus ~130 my) or metamorphic basement; grades upwards conformably into Meramangye Formation or Murnaroo Formation.|Bed of lowstand fluvial conglomerate; white, grey and pink, generally poorly sorted, very fine to very coarse grained quartz sandstone; locally pyritic, dolomitic, with lithic granules to pebbles; minor interbedded red-brown and green siltstone.|17-FEB-15
22953|Tarlina Sandstone|72478|6|Mentioned|p8|Marinoan|Sturtian|Officer Basin.|c. 650 Ma|Lake Maurice Group||Unconformably overlain by Meramangye Formation. Overlain by the Murnaroo Formation.||24-MAR-21
22953|Tarlina Sandstone|73099|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Officer Basin.||Lake Maurice Group.||Is overlain by Meramangye Formation.|Medium-brown, very fine- to fine-grained, quartz and feldspathic quartz sandstone; minor siltstone, claystone and very coarse sandstone.|
22953|Tarlina Sandstone|73392|6|Mentioned|p3||||||||Sampled from core of Giles 1 well.|
24016|Tathra Quartz Diorite|42884|2|Defined|p16|Early Ordovician|Late Cambrian|of Summerfield Intrusive Suite, see also Fig.2 P13||||||
33660|Teal Flat Volcanics|22945|5|Briefly described|p8|||Mentioned under - Area C geology.||||||
33660|Teal Flat Volcanics|23731|6|Mentioned|p43, p51|||||||||
33660|Teal Flat Volcanics|24509|5|Briefly described|p42, p39 Fig. 1, p41 Fig. 2b|Cambrian|Cambrian|Age: ~521Ma. Mafic. Alkaline volcanics. Interbedded with Kanmantoo Group. Range from basalt to andesite in bulk composition; interpreted as primary lava flows. Highly sheared, resulting in mylonitisation; low-T alteration.||||||04-MAY-05
33660|Teal Flat Volcanics|60567|2|Defined|p37|Early Cambrian|Early Cambrian|Originally interpreted as undifferentiated greywackes of the Kanmantoo Group (Steel, 1962). Vary from calc-alkaline basalt to andesite. Age: ~521+/-4Ma and 526+/-Ma. Geological Province: Adelaide Geosyncline.||||||
33660|Teal Flat Volcanics|67536|4|Described|Map Legend|Sandbian|Stage 2|Kanmantoo Province; basement to Murray Basin.|ca. 521 +/- 4 Ma - 478 +/- 23 Ma|||Intercalated with Kanmantoo Group metasediments|Felsic-intermediate volcanic rocks.|
33660|Teal Flat Volcanics|70125|6|Mentioned|p400 Tb.5||||521 Ma.|||||
33660|Teal Flat Volcanics|71322|5|Briefly described|p52 Fig.1, p73|Cambrian|Cambrian|Appears as Teale Flat Volcanics on p73.|521+/-4 Ma - 478+/-3 Ma.|||Intercalated with Normanville and/or Kanmantoo Group.|Felsic-intermediate volcanics.|
33660|Teal Flat Volcanics|73093|5|Briefly described|map legend|Cambrian|Cambrian||||||Basaltic to dacitic metavolcanics.|09-DEC-21
22961|Teizi Anorthosite|43052|5|Briefly described|p160|||of Giles Complex||||||
29847|Telechie Sulphide Member|22884|2|Defined|p40 Fig. 1, p47||Paleoproterozoic|Of the Mount Howden Formation (Paragon Group) occurring at the contact with the underlying Mustering Paddock Formation. Formerly known as "Bimba formation" (Hemming and Lewis 1979). Max. thickness: 20m. Detailed lithology included.||||||26-MAR-09
29847|Telechie Sulphide Member|70405|5|Briefly described|p27|Paleoproterozoic|Paleoproterozoic|Some contention as to which group (out of Mount Howden or Bimba Formation) it belongs to, current consensus is Bimba Formation.||Bimba Formation||Overlies Peryhumuck Formation|Oxidised sulphidic metasediments (gossans).|
37348|Teltawongee Group|23889|5|Briefly described|p35 Fig. 30|Cambrian|Cambrian|||||||
37348|Teltawongee Group|65381|5|Briefly described|p689 Fig.2|Middle Cambrian|Early Cambrian|Variation on Teltawongee beds.||||||
37348|Teltawongee Group|66623|1|Redefined|p17, pp30-49, p348.|Early Cambrian|Early Cambrian|Formerly part of Packsaddle Series (Andrews 1922), Wonominta beds (Warris 1967) and Complex (Scheibner 1972), part of Teltawongee beds (Mills 1992). Approximate equivalents with Kanmantoo Group. Low hills and rises. Geophysical properties described.|504.5 +/- 2.6 Ma (Black 2006).||Includes Nundora, Copper Mine Range, Wonnaminta, Bunker Creek and Depot Glen Formations.|Overlies Kara Formation of Grey Range Group. Intruded by Bittles Tank Volcanics. Capped by Cordillo Silcrete.|Mainly monotonous sequence of dirty turbiditic, metamorphosed, graded-bedded sandstones of uniform grainsize range and composition, and siltstone; presence of detrital muscovite flakes is characteristic.|
37348|Teltawongee Group|66917|5|Briefly described|Map legend|Cambrian|Cambrian|Does not crop out in the map area.|||Includes Wonnaminta Formation.|||
37348|Teltawongee Group|66918|5|Briefly described|Map legend|Cambrian|Cambrian||||Includes Wonnaminta Formation.|||
37348|Teltawongee Group|66921|6|Mentioned|Map legend|||Does not outcrop in map area. Position in cross-section is based on geological interpretation and geophysical modelling.|||Includes Depot Glen Formation.|||
37348|Teltawongee Group|66922|5|Briefly described|Map legend|Cambrian|Cambrian||||Includes Depot Glen Formation.||Well cleaved and folded dark grey to buff-brown fine- to medium-grained turbiditic silty and muddy sandstones, several metres thick, with detrital muscovite to 3 mm; minor grey, green and maroon slate units; metamorphosed to greenschist facies.|
37348|Teltawongee Group|66927|5|Briefly described|Map legend|Cambrian|Cambrian|Narrow, single and paired moderately-magnetic trends which are continuous over many kilometres; mainly occur within Teltawongee Group formations further south (in the Cotham Lake map sheet area).||||||
37348|Teltawongee Group|67105|5|Briefly described|p653-655, 659, 661, 663, 665|Early Cambrian|Early Cambrian|Kayrunnera Zone, Koonenberry Belt.|||Nundora, Wonnaminta, Bunker Creek, Copper Mine Range, Depot Glen Formations.||Metasedimentary rocks; an extensive package of turbiditic sandstones and siltstones.|
37348|Teltawongee Group|67207|5|Briefly described|Map legend.|Cambrian|Cambrian||||Includes Depot Glen Formation.|Overlies Grey Range Group. Is overlain by Ponto Group.|Well cleaved and folded dark grey to buff-brown, fine- to medium-grained turbiditic silty and muddy sandstones, several metres thick; minor grey, green slate and maroon slate units; regionally metamorphosed to greenschist facies.|
37348|Teltawongee Group|67208|5|Briefly described|Map legend.|Cambrian|Cambrian||||Includes Wonnaminta, Depot Glen and Bunker Creek Formations.||Well cleaved and folded, dark grey to buff-brown, fine- to medium-grained turbiditic silty and muddy sandstones, several metres thick, with detrital muscovite to 3 mm; minor grey, green and maroon slate units; greenschist facies.|
37348|Teltawongee Group|67209|5|Briefly described|Map legend.|Cambrian|Cambrian||||Includes Depot Glen Formation.|||
37348|Teltawongee Group|67210|5|Briefly described|Map legend.|Cambrian|Cambrian||||Includes Bunker Creek Formation.|||
37348|Teltawongee Group|67211|5|Briefly described|Map legend.|Cambrian|Cambrian||||Includes Bunker Creek Formation.||Well cleaved and folded dark grey to buff-brown, fine- to medium-grained, turbiditic silty and muddy sandstones, several metres thick, with detrital muscovite to 3 mm; minor grey, green and maroon slate units; metamorphosed to greenschist facies.|
37348|Teltawongee Group|67322|4|Described|p3 Fig.1, p10-13; Fig.5|Cambrian|Cambrian|Koonenberry Belt. Defined by Mills, in Greenfield et al. (2010); previously Teltawongee Beds (Mills, 1992). Occurs in the Wonnaminta and Kayrunnera areas.|||Wonnaminta, Nundora, Bunker Creek, Depot Glen and Copper Mine Range Formations.|Intruded by the Bittles Tank Volcanics.|Consists of weakly metamorphosed graded bedded turbiditic sandstones.|22-FEB-18
37348|Teltawongee Group|68823|6|Mentioned|p376 Fig.3|Cambrian|Cambrian|Separated from Warratta Group by Olepoloko Fault. Mis-spelt as Teltawangee on p400.||||||
37348|Teltawongee Group|69001|6|Mentioned|p2 Fig.1B|Cambrian|Cambrian||||Includes the Depot Glen Formation.|||
37348|Teltawongee Group|69002|6|Mentioned|Map 1b, Legend|Cambrian|Cambrian|Comprises a broad area of low magnetic intensity.|||||Metasediments.|
37348|Teltawongee Group|69042|5|Briefly described|map legends|Cambrian|Cambrian|ETG. Delamerian Orogen. Broad area of low magnetic intensity. Metasediments.||||||
37348|Teltawongee Group|69043|5|Briefly described|p4, p11, p100-101, p104|||NE of the Koonenberry Fault. Deeper-water sedimentary rocks.|||Depot Glen Formation.|||
37348|Teltawongee Group|69541|5|Briefly described|p645 Fig.1(b)|Cambrian|Cambrian||515 Ma.|||||
37348|Teltawongee Group|69961|5|Briefly described|Map legend|Cambrian|Cambrian||||Includes Wonnaminta, Depot Glen and Bunker Creek Formations.||Undifferentiated well-cleaved and folded dark grey to buff-brown, fine- to medium-grained turbiditic silty and muddy sandstones, with detrital muscovite to 3mm; minor grey, green and maroon slate units; regionally metamorphosed to greenschist facies.|
37348|Teltawongee Group|70037|6|Mentioned|p11|||||||||
37348|Teltawongee Group|70210|6|Mentioned|p1|||Koonenberry-Tibooburra district.|||Depot Glen beds.|||
37348|Teltawongee Group|70602|6|Mentioned|p75|Cambrian|Cambrian|||||||
37348|Teltawongee Group|70648|5|Briefly described|Map Legend|Cambrian|Cambrian||||Includes Copper Mine Range Formation, Bunker Creek Formation, Nundora Formation, Wonnaminta Formation.|||
37348|Teltawongee Group|70650|5|Briefly described|Map Legend|Cambrian|Cambrian||||Includes Wonnaminta Formation.|||
37348|Teltawongee Group|70651|5|Briefly described|Map Legend|Cambrian|Cambrian||||Includes Wonnaminta Formation.|||
37348|Teltawongee Group|70744|5|Briefly described|p945|Middle Cambrian|Early Cambrian|Koonenberry Belt. The NE part of this unit is interpreted as a subduction complex.|||||Widespread quartzose turbidites.|
37348|Teltawongee Group|70749|6|Mentioned|p43|Cambrian|Cambrian|Southern Thomson and Koonenberry area.||||||
37348|Teltawongee Group|70838|4|Described|p266, p268-272, p274-278, p280-281|Early Cambrian|Early Cambrian|Koonenberry Belt. Coeval with Ponto Group. Texturally immature: possible tectonic settings discussed (convergent margin preferred). The maximum depositional age is poorly defined from rare trace fossils. Minimum age from intrusion. Deformed during the Delamerian Orogeny (c.500 Ma). Detrital zircon analyses.|>515 +/- 2.7 Ma (Black, 2007).||Bunker Creek, Depot Glen, Wonnaminta and Nundora Formations.|Is faulted against Grey Range Group. Is intruded by Williams Creek Granite. Is overlain unconformably by Kayrunnera Group.|Monotonous packages of poorly sorted sandstone, siltstone and mudstone. Ubiquitous large (<5mm) detrital white mica grains.|
37348|Teltawongee Group|71262|5|Briefly described|p3, p5 Fig 2, p8 Fig 5, p9, p12|Cambrian|Cambrian||||Includes Depot Glen Formation and Bunker Creek Formation|||
37348|Teltawongee Group|71263|6|Mentioned|p18 Fig 2|Cambrian|Cambrian|||||||
37348|Teltawongee Group|71284|5|Briefly described|p487|||Milparinka area, Koonenberry Belt.|||||Includes felsic tuff horizons.|
37348|Teltawongee Group|71415|5|Briefly described|p11,15|Cambrian|Cambrian|Geological province: SW Thomson Orogen. Of the Kooneberry Belt; of Eromanga Basin. Sedimentary sequence related to c. 510 Ma volcanics of the Mount Wright Arc. Underwent deformation and greenschist facies metamorphism during c. 500 Ma Delamarian Orogeny.||||Overlies the Grey Range Group.||19-AUG-19
37348|Teltawongee Group|71593|5|Briefly described|p188|||Koonenberry Province.||||Overlain by the Mount Wright Volcanics. Intruded by the Williams Peak Granite.|Turbiditic sedimentary rocks.|
37348|Teltawongee Group|71860|6|Mentioned|p6|Cambrian|Cambrian|||||||
37348|Teltawongee Group|71965|5|Briefly described|p894,896,901,913|Cambrian|Cambrian|Geological province: Delamerian Orogen. Turbidite deposition to the east, closer to the Thomson Orogen boundary; separated by Olepoloko Fault. Contemporaneous with Mount Wright continental magmatic arc development, and associated c. 510 Ma Gnalta Group and Ponto Group volcanism.||||||
37348|Teltawongee Group|71966|6|Mentioned|p990|Cambrian|Cambrian|Geological province: Delamarian Orogen.||||||
37348|Teltawongee Group|72522|4|Described|p3, p119, p125, p131.|Middle Cambrian|Early Cambrian||||Includes Depot Glen Formation.|Unconformably overlain by Easter Monday Formation. Intruded by Wertago Volcanics.||
37348|Teltawongee Group|72951|6|Mentioned|p1010|||Delamarian Orogen. Koonenberry Belt.||||||
37348|Teltawongee Group|73059|5|Briefly described|p1061|||Considered to be the subduction complex equivalent to the convergent margin arc and forearc deposits represented by the Mount Wright Volcanics. Variation in detrital zircon ages in this unit's constituents indicates their variety of provenances prior to the Delamerian Orogeny.|525-505 Ma.||Nundora, Copper Mine Range Formations.||Deep-marine turbidite succession.|
37348|Teltawongee Group|73093|5|Briefly described|map legend|Cambrian|Cambrian||||||Well-cleaved and folded dark-grey to buff-brown fine- to medium-grained turbiditic silty and muddy sandstones; minor grey, green and maroon slate units; regionally metamorphosed to greenschist facies.|09-DEC-21
37348|Teltawongee Group|73177|5|Briefly described|p1097-1100, 1109 Fig.13(a), 1113|Early Cambrian|Early Cambrian|See also p1114-1115 Figs.16-17. Northern Delamerian Orogen. Has many similarities to the Warratta Group.|||Bunker Creek Formation.|Is overlain by Warratta Group. Is intruded by Williams Peak Granite.||
26169|Tepko Granodiorite|42884|2|Defined|p12|Early Ordovician|Late Cambrian|of Summerfield Intrusive Suite, see also Fig.2 P13||||||
29052|Terowie kimberlites|40811|6|Mentioned|p321|||Kimberlites at Terrowie. Informal.||||||
25749|Thackaringa Group|6823|6|Mentioned|p203-205, 206, 233, 234, 236|Palaeoproterozoic|Palaeoproterozoic||ca >1690 Ma|Willyama Supergroup|Includes the Rasp Ridge Gneiss, Alma Gneiss.|Overlies the Thorndale Composite Gneiss, Clevedale Migmatite, Mulculca Formation, Ednas Gneiss and the Redan Gneiss.||26-MAR-22
25749|Thackaringa Group|22463|6|Mentioned|22 fig 27|Statherian|Statherian|Parent Willyama Supergroup Geol province Broken Hill Domain||||||
25749|Thackaringa Group|22575|6|Mentioned|p179 Fig.2|||In the Broken Hill Block.||||||16-JAN-07
25749|Thackaringa Group|22588|6|Mentioned|p85|||||||||
25749|Thackaringa Group|22631|6|Mentioned|table1, p173|Statherian|Statherian|||||||
25749|Thackaringa Group|22641|6|Mentioned|p692|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
25749|Thackaringa Group|22720|6|Mentioned|p 168|||||||||
25749|Thackaringa Group|22771|5|Briefly described|p40,Table12.2p45,45|||||||||
25749|Thackaringa Group|22789|6|Mentioned|p50|||||||||
25749|Thackaringa Group|22857|4|Described|p40, p45 Tb.12.2, p390 App1 Tb.A1.1|Paleoproterozoic|Paleoproterozoic|Of the Willyama Supergroup. Max. thickness: 3000m. Geological Province: Willyama Fold Belt. ||||||07-NOV-08
25749|Thackaringa Group|22884|5|Briefly described|p40 Fig. 1, p41, p43 Fig. 3||Statherian|Age of lower unit is 1699+/-10 Ma. Geological province: Broken Hill Domain.||||||26-MAR-09
25749|Thackaringa Group|22956|6|Mentioned|p147||Proterozoic|||||||
25749|Thackaringa Group|22959|6|Mentioned|p95||Paleoproterozoic|||||||07-NOV-08
25749|Thackaringa Group|22960|6|Mentioned|p90,92||Paleoproterozoic|||||||07-NOV-08
25749|Thackaringa Group|22962|6|Mentioned|p74||Statherian|||||||
25749|Thackaringa Group|22963|5|Briefly described|p69||Paleoproterozoic|Broad correlation with the Fullarton River Group of the Mt Isa Maronan Supergroup.||||||07-NOV-08
25749|Thackaringa Group|22964|6|Mentioned|p56||Proterozoic|||||||
25749|Thackaringa Group|22965|6|Mentioned|p11,14,Fig1||Paleoproterozoic|Contains the Himalaya, Cues, Alders Tank and Lady Brassy Formations.||||||07-NOV-08
25749|Thackaringa Group|22966|5|Briefly described|p2,4||Proterozoic|||||||
25749|Thackaringa Group|22967|5|Briefly described|p25,6,39,41,2||Statherian|||||||
25749|Thackaringa Group|23025|5|Briefly described|p75-6|||||||||
25749|Thackaringa Group|23039|6|Mentioned|p166||Statherian|||||||
25749|Thackaringa Group|23160|6|Mentioned|fig1|||||||||
25749|Thackaringa Group|23223|5|Briefly described|p39|||Described in article as 'Thackaringa group - quartzofeldspathic suite (TG-QS)'. Of the Willyama Supergroup. In the Curnamona Province.||||||16-JAN-07
25749|Thackaringa Group|23248|6|Mentioned|p170, 179|||||||||
25749|Thackaringa Group|23346|6|Mentioned|48|||||||||
25749|Thackaringa Group|23347|6|Mentioned|p51 Tb. 1, p52|||Geological province: Broken Hill Domain. Presented only as Thackaringa in Table 1. Equivalent to parts of Wiperaminga Subgroup.||||||24-MAR-09
25749|Thackaringa Group|23390|6|Mentioned|p8|||||||||
25749|Thackaringa Group|23461|5|Briefly described|p202|||||||||
25749|Thackaringa Group|23912|6|Mentioned|p779|||||||||
25749|Thackaringa Group|24197|5|Briefly described|p29, p62|Paleoproterozoic|Paleoproterozoic|Of Willyama Supergroup. Leucocratic, high in silica and usually albitic; includes lacustrine sedimentary rocks, felsic metavolcanic rocks, shallow granite sills and several varieties of iron formations. Age: ~1710Ma. Geol.Province: Broken Hill Domain.||||||07-FEB-11
25749|Thackaringa Group|24307|4|Described|p973|Proterozoic|Proterozoic|||||||
25749|Thackaringa Group|38969|4|Described|p204|||||||||
25749|Thackaringa Group|39662|1|Redefined|p414|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
25749|Thackaringa Group|39674|6|Mentioned|p204|||||||||
25749|Thackaringa Group|39826|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
25749|Thackaringa Group|39828|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
25749|Thackaringa Group|39849|6|Mentioned|p87|||||||||
25749|Thackaringa Group|39883|6|Mentioned|p382|||||||||
25749|Thackaringa Group|40290|6|Mentioned|p1|||||||||
25749|Thackaringa Group|40595|6|Mentioned|p78|||||||||
25749|Thackaringa Group|40822|6|Mentioned|Fig.2|||||||||
25749|Thackaringa Group|41093|4|Described|p251|||||||||
25749|Thackaringa Group|41145|5|Briefly described|p827|||||||||
25749|Thackaringa Group|41630|5|Briefly described|p6|||||||||
25749|Thackaringa Group|41633|6|Mentioned|p150|||||||||
25749|Thackaringa Group|41651|5|Briefly described|p190|||||||||
25749|Thackaringa Group|41652|5|Briefly described|p192|||||||||
25749|Thackaringa Group|42171|6|Mentioned|p142|||||||||
25749|Thackaringa Group|42181|6|Mentioned|Fig,1 P252|||||||||
25749|Thackaringa Group|42261|6|Mentioned|Fig 1 P530|||||||||
25749|Thackaringa Group|42286|6|Mentioned|p7|||||||||
25749|Thackaringa Group|42507|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
25749|Thackaringa Group|42527|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
25749|Thackaringa Group|42528|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
25749|Thackaringa Group|42529|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
25749|Thackaringa Group|42530|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
25749|Thackaringa Group|42531|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
25749|Thackaringa Group|42537|3|Fully described|p8|||||||||
25749|Thackaringa Group|42595|6|Mentioned|Fig. 2 P5|||||||||
25749|Thackaringa Group|42720|5|Briefly described|map legend|Paleoproterozoic||||||||07-NOV-08
25749|Thackaringa Group|42813|6|Mentioned|p9|||||||||
25749|Thackaringa Group|42897|5|Briefly described|Fig.3, P321|||||||||
25749|Thackaringa Group|42942|6|Mentioned|p17|||of Willyama Supergroup||||||
25749|Thackaringa Group|43052|6|Mentioned|p84|||||||||
25749|Thackaringa Group|43086|6|Mentioned|Fig.3|||||||||
25749|Thackaringa Group|43263|6|Mentioned|Map Legend||Paleoproterozoic|||||||07-NOV-08
25749|Thackaringa Group|43264|5|Briefly described|Map Legend||Paleoproterozoic|Within the Willyama Supergroup.||||||07-NOV-08
25749|Thackaringa Group|43265|5|Briefly described|Map Legend||Paleoproterozoic|Within the Willyama Supergroup.||||||07-NOV-08
25749|Thackaringa Group|43266|5|Briefly described|Map Legend||Paleoproterozoic|Within the Willyama Supergroup.||||||07-NOV-08
25749|Thackaringa Group|43267|5|Briefly described|Map Legend||Paleoproterozoic|Within the Willyama Supergroup.||||||07-NOV-08
25749|Thackaringa Group|43268|5|Briefly described|Map Legend||Paleoproterozoic|Within the Willyama Supergroup.||||||07-NOV-08
25749|Thackaringa Group|43270|5|Briefly described|Map Legend||Paleoproterozoic|Of the Willyama Supergroup.||||||07-NOV-08
25749|Thackaringa Group|43271|5|Briefly described|Map Legend||Paleoproterozoic|Of the Willyama Supergroup.||||||07-NOV-08
25749|Thackaringa Group|43272|5|Briefly described|Map Legend||Paleoproterozoic|Of the Willyama Supergroup.||||||07-NOV-08
25749|Thackaringa Group|43273|5|Briefly described|Map Legend||Paleoproterozoic|Of the Willyama Supergroup.||||||07-NOV-08
25749|Thackaringa Group|43274|5|Briefly described|Map Legend||Paleoproterozoic|Of the Broken Hill Group.||||||07-NOV-08
25749|Thackaringa Group|43572|6|Mentioned|p5|||||||||
25749|Thackaringa Group|43583|5|Briefly described|Table 1, p2139|||||||||
25749|Thackaringa Group|43595|5|Briefly described|p355|||||||||
25749|Thackaringa Group|46598|4|Described|p303|||||||||
25749|Thackaringa Group|50045|4|Described|p116 Fig. 3, p115 Fig. 2|Statherian|Statherian|Geol Prov: Broken Hill Block. Of  Willyama Supergroup. Conformably overlain by Broken Hill Group; underlain by Thorndale Composite Gneiss and Mulculca Formation. Age: c.1710 Ma. Includes 7 named units.||||||31-MAY-07
25749|Thackaringa Group|50606|5|Briefly described|p1.1|||Geological Province: Broken Hill Block. Of the Willyama Supergroup. Intruded by Potosi Supersuite.||||||
25749|Thackaringa Group|50619|5|Briefly described|p174 Fig. 1|Paleoproterozoic|Paleoproterozoic|Of the Willyama Supergroup.  Interbedded psammite, pelite and quartz-albitite.  Conformably overlain by the Broken Hill Group.  Geological Province: Broken Hill Block.||||||07-NOV-08
25749|Thackaringa Group|60485|5|Briefly described|p28 Fig. 2|||Geological Province: Broken Hill Domain.||||||03-MAR-05
25749|Thackaringa Group|61258|5|Briefly described|p399|Paleoproterozoic|Paleoproterozoic|Includes the Himalaya and Alma Formations. Geological Province: Broken Hill-Olary region.||||||07-NOV-08
25749|Thackaringa Group|61262|5|Briefly described|p455 Fig. 11|Paleoproterozoic|Paleoproterozoic|Age: >1700Ma. Geological Province: Broken Hill.||||||07-NOV-08
25749|Thackaringa Group|61605|5|Briefly described|p769|Paleoproterozoic|Paleoproterozoic|Of the Willyama Supergroup. Geological Province: Broken Hill domain.||||||07-NOV-08
25749|Thackaringa Group|61606|5|Briefly described|p4 Fig.2|||Of the Willyama Supergroup.||||||18-MAY-06
25749|Thackaringa Group|61735|5|Briefly described|p635 Fig. 1, p636, 640|Paleoproterozoic|Paleoproterozoic|Oldest recognised part of the Willyama Supergroup. Age: 1730-1720Ma. See also p636 Fig. 2. Regional metamorphism 1595+/-6 Ma U/Pb SHRIMP.||||||04-JUN-15
25749|Thackaringa Group|61736|5|Briefly described|p666 Fig. 3|Paleoproterozoic|Paleoproterozoic|Contains Lady Brassey, Cues and Himalaya Formations, Geological province: Olary Domain.||||||
25749|Thackaringa Group|62373|5|Briefly described|p503|Paleoproterozoic|Paleoproterozoic|Of the Willyama Supergroup. Migmatised, quartz-feldspathic rocks and albite-quartz rocks. Geological Province: Curnamona Province/Olary Domain.||||||07-NOV-08
25749|Thackaringa Group|62473|5|Briefly described|p72|Paleoproterozoic|Paleoproterozoic|Age: 1710-1700ma. Geological province: Broken Hill Domain.||||||17-JUN-09
25749|Thackaringa Group|62535|5|Briefly described|p665, p667, p670, p672-674|Paleoproterozoic|Paleoproterozoic|Hosts Broken Hill-type base metal deposits.|c.1720 Ma.||Lady Brassey, Cues, Himalaya Formations.|||
25749|Thackaringa Group|62536|4|Described|p633, 635-638, 640, 642, 647, 653, 658|||Broken Hill area. A minimum age for the lower part of this unit is 1704 +/- 3 Ma. Contains various metal ores (listed).|1720 Ma (MDA).|Willyama Supergroup.|Himalaya, Cues, Alders Tank, Lady Brassey Formations; Alma Gneiss.|Overlies Thorndale Composite Gneiss. Is intruded by Alma Gneiss and Farmcote leucogneiss.||
25749|Thackaringa Group|62592|5|Briefly described|p14, p16, p16 Fig.2.2.|||Broken Hill Domain, Curnamona Province. This unit, representing a >10 m.y. gap, is missing from the Olary Domain.||Unit in Willyama Supergroup.|Includes Thorndale Composite, Redan and Ednas Gneisses; Clevedale Migmatite; Mulculca, Lady Brassey, Kyong, Alders Tank, Cues and Himalaya Formations.|Is intruded by Alma and Rasp Ridge Gneisses.||
25749|Thackaringa Group|62728|5|Briefly described|p25 Fig. 2|||Includes the Thackeringa Group metasediments. Geological Province: Curnamona Province.||||||07-FEB-11
25749|Thackaringa Group|62993|5|Briefly described|p35, p37|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain.||Willyama Supergroup|Includes Himalaya Formation, Cues Formation, Alders Tank Formation, Lady Brassey Formation|||19-DEC-21
25749|Thackaringa Group|63020|5|Briefly described|p987 Fig. 8|Paleoproterozoic|Paleoproterozoic|Geological Province: Curnamona Province (Broken Hill Domain).||||||07-NOV-08
25749|Thackaringa Group|63102|5|Briefly described|p13|Statherian|Statherian|Geological province: Broken Hill Domain, Curnamona Province.|||Includes Himalaya Fm, Kyong Fm, Cues Fm, Alders Tank Fm, Lady Brassey Fm, Thorndale Composite Gneiss, Mulculca Fm, Clevedale Migmatite, Ednas Gneiss and Regan Gneiss.|||
25749|Thackaringa Group|63110|6|Mentioned|p1129 Fig. 8, p1131|||Comprises metasedimentary rocks with intrusive, shallow level granitoids.||||||
25749|Thackaringa Group|63186|5|Briefly described|p66, p67, p71 Fig. 5|Paleoproterozoic|Paleoproterozoic|Of the Willyama Supergroup. Age: 1705Ma. Geological Province: Broken Hill Domain, Curnamona Province. Intruded by Rasp Ridge and Hores Gneisses. Lower section includes Cues Formation.||||||07-NOV-08
25749|Thackaringa Group|63489|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Metasediments, composite gneiss, albite-rich rocks, granitic gneiss, amphibolite, minor quartz-magnetite rocks and metasediments in Broken Hill Domain; equivalent metasediments in Olary Domain.||||||07-NOV-08
25749|Thackaringa Group|63519|5|Briefly described|p5, p10 Fig. 3|Paleoproterozoic|Paleoproterozoic|Includes Alma Gneiss, Lady Brassey, Alders Tank, Cues Formations and Himalaya Formations, and Rasp Ridge Gneiss. Albite rock. ||||||07-NOV-08
25749|Thackaringa Group|63866|5|Briefly described|p36, p38, p40|||Broken Hill Domain, Curnamona Province.|1705-1693 Ma||Includes the Lady Brassey Formation, Cues Formation and the Himalaya Formation.|||
25749|Thackaringa Group|64097|5|Briefly described|p302, p306|Paleoproterozoic|Paleoproterozoic|Of Willyama Supergroup. Includes Alma Gneiss, Lady Brassey Fm.(both basal), Alders Tank,Cues and Himalaya Formations. Overlies Thorndale Composite Gneiss; underlies Broken Hill Group. Max. age: ca 1720Ma. Abundant albitised metasediment.||||||07-FEB-11
25749|Thackaringa Group|64250|6|Mentioned|p25 fig 10|||||Unit in Willyama Supergroup.||||
25749|Thackaringa Group|64316|5|Briefly described|p532, p533 Fig. 1|Paleoproterozoic|Paleoproterozoic|Of the lower Willyama Supergroup. Includes Lady Brassey, Cues and Himalaya Fms. Migmatised quartzo-feldspathic rocks and albititeswith progressive increase in poelitic-trubiditic component up into the broken Hill Group above. Geol.Prov: Broken Hill Block.||||||07-FEB-11
25749|Thackaringa Group|64722|5|Briefly described|Fig. 5 p.13|Statherian|Statherian|Broken Hill region, South Australian Craton.||Of Willyama Supergroup.||||11-APR-12
25749|Thackaringa Group|64725|6|Mentioned|p58 Fig.2. |||||||||
25749|Thackaringa Group|64741|5|Briefly described|p301 Fig. 4, p307|Paleoproterozoic|Paleoproterozoic|Of Willyama Supergroup. Overlain by Broken Hill Group. Geological province: Broken Hill Domain.||||||07-FEB-11
25749|Thackaringa Group|64742|5|Briefly described|p320 Fig.2, p328.|||Broken Hill Domain. Major and trace element analyses, and Sm-Nd isotope data, are detailed.||Unit in Willyama Supergroup.|Includes Lady Brassey, Cues, and Himalaya Formations.|||29-MAR-12
25749|Thackaringa Group|64743|6|Mentioned|pp339-340, p344 Fig.5. |Paleoproterozoic|Paleoproterozoic|||Unit in Willyama Supergroup.||Is overlain by Broken Hill Group.||
25749|Thackaringa Group|64744|5|Briefly described|p353 Fig.4, p354. |Statherian|Statherian|Broken Hill Domain.||Unit in Willyama Supergroup.||Is intruded by Alma and Rasp Ridge Gneisses. Is overlain by Broken Hill Group.|Psammopelitic schists and gneisses.|
25749|Thackaringa Group|64944|5|Briefly described|p28 Fig. 1|Paleoproterozoic|Paleoproterozoic|Includes Lady Brassey, Alders Tank, Cues and Himalaya Formations. Geological province: Broken Hill Domain.||||||07-FEB-11
25749|Thackaringa Group|65681|6|Mentioned|pp733-734,|Paleoproterozoic|Paleoproterozoic|||Unit in Willyama Supergroup.|Previously regarded as including Rasp Ridge Gneiss.|||16-MAY-13
25749|Thackaringa Group|65925|5|Briefly described|Appendix 2.||||Includes metavolcanics 1699+/-10 Ma. ||||Gneiss, quartz-feldspar-biotite, foliated; calc-albitite and quartz-plagioclase rich metasediment; metavolcanics 1699+/-10 Ma; ironstone; calc-silicate; minor Pb-Zn-Ag-Cu mineralisation; minor amphibolite.|
25749|Thackaringa Group|66302|5|Briefly described|p35, p36 Fig.9, p37, p38, p39, p40|Statherian|Statherian|Olary and Broken Hill Domains, Curnamona Province.|1705-1693 Ma (Conor, 2006)|Willyama Supergroup|Includes the Thorndale Composite Gneiss, Clevedale Migmatite, Lady Brassey Formation, Alders Tank Formation, Cues Formation and Himalaya Formation.|Overlain by the Broken Hill Group. Intruded by the Silver City Suite.||
25749|Thackaringa Group|66857|5|Briefly described|p971, p972 Fig.2.|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain. Thought to have equivalents in the (informally-named) Quartzo-feldspathic Suite of the Olary Domain.|c.1700 Ma (Ashley et al. 1997).|Unit in Willyama Supergroup.||Overlies Thorndale Composite Gneiss. Is overlain by Broken Hill Group.||
25749|Thackaringa Group|67323|5|Briefly described|Eastern Australia Time-Space Plot; p33|||Broken Hill Domain, Curnamona Province. Deposited during intra-continental extension.|||Himalaya, Cues, Lady Brassey Formations; Thorndale Composite Gneiss.|Is overlain by Broken Hill Group.||
25749|Thackaringa Group|68067|6|Mentioned|Map legend.|||Areas with higher magnetic response are mapped separately.||||||27-AUG-13
25749|Thackaringa Group|68126|5|Briefly described|p6, p26, p29-30|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain, Curnamona Province.|c.1710-1700 Ma (maximum depositional age).|Willyama Supergroup.||Is overlain by Broken Hill Group.||
25749|Thackaringa Group|69999|5|Briefly described|p3, p9 Photo 11, p14, p16-18, p20|Paleoproterozoic|Paleoproterozoic|Curnamona Province. Basal, early-rift fluviatile to shallow marine sedimentation. Orthopyroxene -bearing rather than garnet-bearing, unlike Broken Hill Group: discussed.||||||
25749|Thackaringa Group|70000|5|Briefly described|p31, p33-37|Statherian|Statherian|||Unit in Willyama Supergroup.|Includes Lady Brassey, Cues and Himalaya Formations.|Is overlain conformably by Broken Hill Group.|Contains a sequence of variably albitic, psammite-dominated metasedimentary rocks.|
25749|Thackaringa Group|70014|5|Briefly described|Map legend|||||Unit in Willyama Supergroup.||Overlies Thorndale Composite Gneiss and Mulculca Formation. Is overlain by Broken Hill Group.|Characterised by a wide variety of quartzo-feldspathic lithologies, including quartz-feldspar-biotite gneisses and leucocratic plagioclase-quartz rocks, as well as composite gneiss, lesser metasediment, and sporadic to abundant basic gneiss bodies.|
25749|Thackaringa Group|70015|5|Briefly described|Map legend|Statherian|Statherian|Mineral deposits (if any) are shown.||Unit in Willyama Supergroup.|Includes Lady Brassey, Cues and Himalaya Formations.|Is overlain by Broken Hill Group.|Sodic plagioclase-quartz rocks at top and base, with intervening metasedimentary rocks and composite gneiss; intruded by granitic and basic gneiss.|
25749|Thackaringa Group|70405|6|Mentioned|p15, p43 Table 3, p92|Mesoproterozoic|Paleoproterozoic|Correlated with Curnamona group previously (now known to be incorrect).|1700 Ma|Wilyama Supergroup|Includes Cues Formation, Himalaya Formation, Alders Tank Formation, Lady Brassey Formation||Low magnetic intensity.|
25749|Thackaringa Group|70657|4|Described|p6 Fig.1, p10 Fig.4, p11 Fig.5, p12|Statherian|Statherian|See also p13 Fig.6, p15. Curnamona Province; Mulyungarie, Broken Hill Domains. Shown as Thackaringa Group + Thorndale Composite Gneiss + Clevedale Migmatite in Fig.4.|~1705-1700 Ma|Lower Willyama Supergroup|Includes Thorndale Composite Gneiss; Lady Brassey, Alders Tank, Cues, Himalaya Formations.|Overlies Redan and Farmcote Gneisses (Rantyga Group). Underlies Allendale Metasediments (Broken Hill Group). Intruded by Silver City Suite.||
25749|Thackaringa Group|70658|5|Briefly described|p2, 15-|Paleoproterozoic|Paleoproterozoic|Broken Hill region.|1705-1700 Ma.|Willyama Supergroup.|Lady Brassey, Alders Tank, Cues, Himalaya Formations.|Associated with Silver City Suite.||
25749|Thackaringa Group|71968|6|Mentioned|p4|||Geological province: Curnamona province.||||||
25749|Thackaringa Group|72004|6|Mentioned|p84|||Broken Hill region. May have been volcanics, altered in an alkaline environment, most likely an evaporitic setting.|||Includes Himalaya Formation.|Overlain by Willyama Supergroup.||
25749|Thackaringa Group|72435|6|Mentioned|p715|||||||||
25749|Thackaringa Group|72454|6|Mentioned|p2 Fig.2, p8 Fig.6|Mesoproterozoic|Mesoproterozoic|Part of the Broken Hill Domain.  Shown only on p2 Fig.2 and p8 Fig.6.||Willyama Supergroup||||
25749|Thackaringa Group|72461|4|Described|p5-6, p13, p16|||Some of the oldest sedimentary rocks in the  Curnamona Craton (Broken Hill Block). Hosts Great Eastern-type Copper Cobalt mineralisation.||Willyama Supergroup|Includes the Himalaya Formation, Lady Brassey Formation, Cues Formation.|Overlain by the Broken Hill Group.||
25749|Thackaringa Group|73021|5|Briefly described|p224||||~1710 Ma to ~1704 +/- 3 Ma.|Willyama Supergroup.|Cues Formation.|||
25749|Thackaringa Group|73243|6|Mentioned|p52 Fig.1, p53 Fig.2, p59, p65-66, p76|Statherian|Statherian|Broken Hill block-Euriowie block. Amphibolite bodies are mostly concordant or near-concordant with bedding, interpreted as sills emplaced during or immediately after deposition of the Broken Hill Group. Amphibolite is used in text to refer to all highly metamorphosed pre-1600 Ma mafic rocks including hornblende granulites and pyroxene granulites.|~1705-1700 Ma|Willyama Supergroup|Cues Formation, Lady Brassey Formation||Contains amphibolite sills.|
25749|Thackaringa Group|73308|6|Mentioned|p606-607||||c.1705-1700 Ma.|Willyama Supergroup.||||
25749|Thackaringa Group|73429|5|Briefly described|p106 Fig.2, p107|Statherian|Statherian|Curnamona Province, Broken Hill Domain.||Willyama Supergroup, lower|Lady Brassey Formation, Alders Tank Formation, Cues Formation, Himalaya Formation|||
25749|Thackaringa Group|73482|5|Briefly described|p422 Fig.3, p425-426, p430, p432-433|||Hosts pegmatitic masses. See also p423.||Willyama Supergroup|Lady Brassey Group, Cues Formation, Himalaya Formation||Metasediments.|
25749|Thackaringa Group|73512|5|Briefly described|p2-7|Statherian|Statherian|Curnamona Province, Broken Hill Block. Fluviatile to shallow marine successions. Monozite U-Pb SHRIMP age of 1636.8 +/- 4.4 Ma reflects an amphibolite-facies pre-Olarian metamorphic event.||Willyama Supergroup|Cues Formation|Overlain by Broken Hill Group.|Includes metapelites.|
25749|Thackaringa Group|73524|5|Briefly described|p2, p5 Fig.3|||Rift-phase metasediments.||lower Willyama Supergroup|Cues Formation, Lady Brassey Formation, Thorndale Composite Gneiss, Clevedale Migmatite|||16-FEB-23
25749|Thackaringa Group|73575|5|Briefly described|p828 Fig.2, p829 Fig.3, p830, p838|||||Willyama Supergroup|Lady Brassey Formation, Cues Formation, Himalaya Formation|Overlies Thorndale Composite Gneiss, underlies Broken Hill Formation, Allendale Metasediments||
24519|Third Plain Creek Member|40672|5|Briefly described|p5|||||||||
24519|Third Plain Creek Member|42226|4|Described|p232|||||||||
24519|Third Plain Creek Member|44133|6|Mentioned|p24|||Of Clarke, 1986b. Of the Mernmerna Formation.||||||
24519|Third Plain Creek Member|60418|5|Briefly described|p135|Botoman-Atdabanian|Botoman-Atdabanian|Thickness: 233m. Interbedded limestones and shales, with some sandy and silty lithologies. Of Mernmerna Formation.||||||
24519|Third Plain Creek Member|62784|5|Briefly described|p9|Early Cambrian|Early Cambrian|Unit in the middle Mernmerna Formation of Hawker Group, Arrowie Basin. Contains abundant silicified and phosphatic macro- and micro-fossils.|||||Interbedded black turbiditic wackestone-packstone, laminated lime silt and mud, rare sandstone beds.|20-MAR-12
24519|Third Plain Creek Member|63569|5|Briefly described|p117, p119, pp122-123, p124, p127, 136|Early Cambrian|Early Cambrian|Deposited in anaerobic and dysaerobic zones of the lower slope. Contains silicified assemblage of Pararaia bunyerooensis Zone.||Unit in middle Mernmerna Formation.||||
24519|Third Plain Creek Member|70833|5|Briefly described|p185,198,200|Series 2|Series 2|Of Arrowie Basin. Key section: MMT (Bunkers Range, central Flinders Ranges); ||Unit of Mernmerna Formation.||Lowermost unit of Mernmerna Formation. Overlain by Linns Springs Member.||
24519|Third Plain Creek Member|70835|6|Mentioned|p336, 349, 353-355|Cambrian|Cambrian|Arrowie Basin, Flinders Ranges. Type section is in Wilkawillina Gorge in the Bunkers Graben. Contains helcionellid mocrofossils (systematic paleontology descriptions/photographs).||Mernmerna Formation.||Overlies Linns Springs Member conformably or Winnitinny Creek Member (Wilkawillina Limestone) unconformably. Is overlain by Bunkers Sandstone.||
24519|Third Plain Creek Member|71102|5|Briefly described|p244-246,251,256|Series 2|Series 2|Of Arrowie Basin. Nomenclature of Clarke (1986b, 1990a) in the Bunkers Graben and Range; variably developed in the Arrowie Basin. Intersected sections: DBS (Donkey Bore Syncline), MMF (Bunkers Range, Central Flinders Ranges), 10MS (10 Mile South, Bunkers Graben). Variably developed within the Arrowie Basin.||Unit of Mernmerna Formation.||Underlain by Linns Springs Member, or disconformably by Wilkawillina Limestone..||
24520|Thora Dolomite|22510|6|Mentioned|p41|||Of the Upalinna Subgroup.  ? not shown in Table 1.||||||13-OCT-04
24520|Thora Dolomite|23054|5|Briefly described|p14-5|||Coats and Preiss (1987b) suggested that this unit could be regarded as a local member of the Amberoona Formation.||||||
24520|Thora Dolomite|36733|2|Defined|p71|Adelaidean|Adelaidean|See also P51.||||||
24520|Thora Dolomite|38108|6|Mentioned|Table 1|||||||||
24520|Thora Dolomite|41405|5|Briefly described|p172|||||||||
24520|Thora Dolomite|43052|6|Mentioned|p189|||||||||
24520|Thora Dolomite|44289|5|Briefly described|Map Legend||Proterozoic|||||||
24520|Thora Dolomite|71895|6|Mentioned|APP4. p4, |||Punt Hill Region.||||||
67983|Throoka Silt|44133|5|Briefly described|p164, 165 Fig. 10.11|Late Eocene|Late Eocene|Correlative Of the Clinton Formation. Geological Province: Saint Vincent Basin. ||||||
67983|Throoka Silt|60958|5|Briefly described|Map Legend|Eocene|Eocene|Pale grey to light brown siltstone and basal trough cross-bedded, haematitic fine grained sandstone. Geological Province: Saint Vincent Basin.||||||
67983|Throoka Silt|61121|5|Briefly described|Map legend|Eocene|Eocene|Pale grey to light brown siltstone and basal trough cross-bedded, haematitic fine-grained sandstone; foraminifera.  Geological Province: St. Vincent Basin.||||||
67983|Throoka Silt|65375|4|Described|p35.|Eocene|Eocene|[Formal name is Throoka Silts]. Interpreted as lagoonal deposits; shows thin-bedding, lamination, minor cross-bedding, silicified wood and plant impressions.||||Basal channel deposits are incised into Muloowurtie Formation. Grades laterally into Blanche Point Formation. Is overlain unconformably by Rogue Formation.|A 2.3 - 3.6m thick bed of lagoonal pale grey to light brown siltstone and fine-grained sandstone; locally with basal trough cross-bedded, haematitic sandstone.|
67983|Throoka Silt|67462|5|Briefly described|Map legend.|Eocene|Eocene|Western Saint Vincent Basin.||||Overlies Muloowurtie Formation. Is overlain by Rogue Formation.||
67983|Throoka Silt|68715|6|Mentioned|p31 Fig.5|Bartonian|Bartonian|St Vincent Basin.||||||
67983|Throoka Silt|70382|6|Mentioned|p28, p30|||Geological province: St Vincent Basin. Hosts spectacular paleoredox interfaces defined as goethite hematite transitions that in some cases define roll-fronts.||||||
26941|Tickera Granite|22430|6|Mentioned|p2||Proterozoic|||||||
26941|Tickera Granite|22613|6|Mentioned|p29|||||||||
26941|Tickera Granite|22629|5|Briefly described|fig2, p,152,158|Calymmian|Calymmian|1600-1575Ma||||||
26941|Tickera Granite|23719|4|Described|p23|Mesoproterozoic|Mesoproterozoic|See also page 16 table 3, page 17 table 4. Of Hiltaba Suite. Geological Province: Gawler Craton.||||||
26941|Tickera Granite|24197|5|Briefly described|p30, p74 Tb. 8.1|Mesoproterozoic|Mesoproterozoic|Of the Hiltaba Suite (Roxby Downs type). Age: 1592Ma. Geological Province: Gawler Craton.||||||07-FEB-11
26941|Tickera Granite|24475|5|Briefly described|p46|Mesoproterozoic|Mesoproterozoic|Of Hiltaba Suite.||||||
26941|Tickera Granite|24585|5|Briefly described|p32|Calymmian|Calymmian|Intrudes the Wallaroo Group. Age: 1598-1586Ma.||||||23-DEC-09
26941|Tickera Granite|31845|6|Mentioned|p6|||Carpentarian||||||
26941|Tickera Granite|35678|6|Mentioned|Fig.2|||Geological cross-sections, northern Yorke Peninsula.||||||
26941|Tickera Granite|39349|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
26941|Tickera Granite|39802|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
26941|Tickera Granite|42235|6|Mentioned|p132|||||||||
26941|Tickera Granite|43052|5|Briefly described|Table 5.6|||of Hiltaba Suite||||||
26941|Tickera Granite|43053|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of Hiltaba Suite. Anorogenic granitoids. Geological Province: Gawler Craton.||||||26-MAY-05
26941|Tickera Granite|43258|5|Briefly described|Map Legend||Mesoproterozoic|||||||
26941|Tickera Granite|43298|6|Mentioned|Map Legend||Mesoproterozoic|||||||
26941|Tickera Granite|50605|5|Briefly described|p(ii), 1.3, 8.1, Table 1.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Gawler Craton & Curnamona Province. Of the Roxby Downs suite (Hiltaba Supersuite). Age: 1598-1575 +/- 7Ma (U-Pb).||||||
26941|Tickera Granite|60953|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of the Hiltaba Suite. Geological Province: Gawler Craton.||||||26-APR-05
26941|Tickera Granite|60958|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of the Hiltaba Suite. Red-brown, medium-grained, I Type monzonite to quartz monzonite. Age: 1598 +/- 7 - 1575 +/- 7Ma. Geological Province: Gawler Craton.||||||14-APR-05
26941|Tickera Granite|61108|5|Briefly described|map legend|Mesoproterozoic|Mesoproterozoic|Of Hiltaba Suite. Geological Province: Gawler Craton. Age: 1598-1575 Ma.||||||23-JUN-05
26941|Tickera Granite|61121|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of Hiltaba SuiteRed-brown, medium-grained, I-type monzonite to quartz monzonite with microcline, quartz, plagioclase, biotite, +/-muscovite, chlorite and magnetite; undeformed to foliated.  Age: 1598+/-7-1575+/-7Ma. Geological Province: Gawler Craton.||||||02-JUN-05
26941|Tickera Granite|63398|5|Briefly described|p663, p665 Fig 4(e)|Mesoproterozoic|Paleoproterozoic|Of the Hiltaba Suite. Intruded the Wallaroo Group. Geological Province: Gawler Craton. Contains several phases including red-brown adamellite or monzogranite, minor granodiorite and light grey tonalite-trondhjemite.||||||07-NOV-08
26941|Tickera Granite|64130|5|Briefly described|p1387 ||||1577 +/- 7 Ma (Conor, 1995; Fanning et al., 2007)|||Emplacement synchronous with deformation of the Wallarro Group.||
26941|Tickera Granite|65375|4|Described|p13, p21, pp23-24.|Mesoproterozoic|Mesoproterozoic|North Yorke Peninsula. Equivalent to Arthurton Granite in central area. The Tiparra Deformation, c.1585 Ma, formed NE and NW-trending fault-shear zones.|c.1598-c.1560 Ma.|||Intrudes Wallaroo Group.|Two phases: red-brown monzonite or quartz monzonite, consisting mainly of microcline and quartz with minor plagioclase, biotite, +/- muscovite and magnetite; and light grey tonalite, in which plagioclase and quartz are dominant.|
26941|Tickera Granite|65376|4|Described|pp112-116, p147. |||Contains inherited zircons aged c.1763 Ma, possibly from Moonta Porphyry, Wardang and Mona Volcanics Members.|1591 +/- 19 Ma to 1577 +/- 7 Ma.|Unit in Hiltaba Suite.|||Composite body including granite, I-type leucomonzonite and S-type leucotonalite; generally strongly deformed.|
26941|Tickera Granite|65390|5|Briefly described|p18, p23 Fig.3, p26 Tb. 1|Mesoproterozoic|Mesoproterozoic|Olympic Domain, Gawler Craton. Of Hiltaba Suite. Intrudes Doora Schist. Coarse-grained granite-adamellite. Aged 1215 +/- 554 Ma, IR=0.7357 (Rb-Sr: Webb et al., 1986).||||||
26941|Tickera Granite|66302|6|Mentioned|p47|Calymmian|Calymmian|Olympic Domain, Gawler Craton.|1577 +/- 7 Ma (Creaser and Cooper, 1993)|Hiltaba Suite||Intrudes the Wallaroo Group.||
26941|Tickera Granite|67900|6|Mentioned|p22|||Moonta region, SW Gawler Craton. Associated with the Kararan Orogeny.|1577 +/- 7 Ma (Conor, 1995).|||||
26941|Tickera Granite|69748|5|Briefly described|p179-180, 182, 185-198|Mesoproterozoic|Mesoproterozoic|Moonta-Wallaroo region, Olympic IOGC Province. Synchronous with the Kararan Orogeny. Photomicrographs. REY fractionation trends graphed. LA-CP-MS data for REE, Pb, Th, U and other elements tabulated.|1598 +/- 7 Ma to 1575 +/- 7 Ma.|Hiltaba Suite.|||Forms composite batholiths comprising monzogranite and granodiorite to tonalite. I- and S-type. Intensely deformed.|
26941|Tickera Granite|70334|5|Briefly described|p75|Calymmian|Calymmian|Geological province: Gawler Craton. Emplaced at 1577+\-7 Ma (Conor 1995; Fanning et al., 2007), synchronous with Wallaroo Group deposition during 1590-1555 Ma Kararan Orogeny.|1577+\-7 Ma (emplacement)|||||
26941|Tickera Granite|70382|6|Mentioned|p33|||Crops out in northeastern Yorke Peninsula. Possible source for some of Quartoo Sand Member inherited zircon.||||||
26941|Tickera Granite|70659|5|Briefly described|p4|Mesoproterozoic|Mesoproterozoic||~1575 Ma|Hiltaba Suite.||Intrudes Wallaroo Group.||
26941|Tickera Granite|72065|5|Briefly described|p105|Calymmian|Calymmian|Geological province: Gawler Craton. Emplacement age at 1597+\-7 Ma (zircon, U-Pb, SHRIMP, Fanning et al., 2007).||Unit of Hiltaba Suite.||||
26941|Tickera Granite|72949|6|Mentioned|p36|Calymmian|Statherian|Olympic Domain, south. Yorke Peninsula / Eastern Eyre Peninsula. A-type (alkali-calcic) granite.|1597 +/- 7 Ma, 1577 +/- 7 Ma|||||
26941|Tickera Granite|73092|6|Mentioned|p50, 54|Calymmian|Statherian|Age is of magmatic crystallisation. Dated sample is foliated granite from drillhole PBD30 (119.4-120.4 m); sample tentatively assigned to this unit based on similar ages and deformation fabric. Misspelt as Tickera Ganite p3.|1577 +/- 25 Ma|Hiltaba Suite|||Dominantly quartz-biotite monzonite. Sample is augen textured foliated granite.|
26941|Tickera Granite|73103|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic||||||Granite-adamellite, coarse-grained.|
26941|Tickera Granite|73165|4|Described|p619-638|Calymmian|Calymmian|Gawler Craton, Moonta Domain, northern Yorke Peninsula. Four phases classified as granite nodules, a quartz alkali-feldspar syenite, a leucotonalite and an alkali-feldspar granite. Quartz alkali-feldspar syenite is recessively weathered, previously referred to as a foliated quartz monzonite, includes the granite nodules as corestones. Red alkali-feldspar granite occurs as a sheeted dyke, previously referred to as a quartz monzonite. Mostly sharp contact boundaries, metasomatism of the leucotonalite is associated with subsequent emplacement of the alkali-feldspar granite phase. Foliation is predominantly NE-trending and steeply dipping. Unit correlated with Hiltaba Suite based on age and geochemistry, potentially derived from a different or heterogeneous source region compared to the broader Hiltaba Suite. Emplacement synchronous with deformation, metamorphism and metasomatism affecting the Wallaroo Group ca 1600-1575 Ma, correlated with the 1600-1585 Ma Olarian Orogeny in the Curnamona Province. Includes metasedimentary xenoliths of Wallaroo Group.|1598 +/- 7 Ma, 1575 +/- 7 Ma|Hiltaba Suite||Intrudes into Wallaroo Group|Brown-red qtz alkali-feldspar syenite w nodules of alkali-feldspar granite, local metasedimentary xenoliths; intruded by white leucotonalite, two cleavages; + later red alkali-feldspar granite; well-developed foliation, hematite + sericite alteration|
24522|Tidnamurkuna Volcanics|22629|6|Mentioned|p152, fig2p147,p153|Statherian|Statherian|1780+/-12 Ma||||||
24522|Tidnamurkuna Volcanics|23054|5|Briefly described|p8-9||Statherian|Max Age: 1780 (+/-) 12 Ma.||||||
24522|Tidnamurkuna Volcanics|23480|5|Briefly described|p21|Paleoproterozoic|Paleoproterozoic|Age: 1780+/-12 Ma (U-Pb)||||||07-NOV-08
24522|Tidnamurkuna Volcanics|24197|5|Briefly described|p75 Tb. 8.1|Paleoproterozoic|Paleoproterozoic|Age: 1806Ma.||||||07-FEB-11
24522|Tidnamurkuna Volcanics|41972|4|Described|p373|||||||||
24522|Tidnamurkuna Volcanics|43052|4|Described|p100|||of Peake Metamorphics. Age of 1780 Ma.||||||13-OCT-08
24522|Tidnamurkuna Volcanics|43583|6|Mentioned|p2163|||Age: 1806+/-27 Ma||||||
24522|Tidnamurkuna Volcanics|44289|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
24522|Tidnamurkuna Volcanics|50605|5|Briefly described|p(iii), 11.1, 11.3|Mesoproterozoic|Paleoproterozoic|Geological Province: Gawler Craton & Curnamona Province. Age: 1806 +/- 27Ma. Maximum Thickness: ~600m.||||||07-NOV-08
24522|Tidnamurkuna Volcanics|65376|4|Described|p10, pp227-236. |Paleoproterozoic|Paleoproterozoic|c.600m thick. Felsic units show geochemical similarities with Myola Volcanics.|1789 +/- 10 Ma. to 1774 +/- 16 Ma.|Unit in Peake Metamorphics.|||Amygdaloidal basalts and rhyolite, interbedded with the predominantly quartzitic sequence of the Baltucoodna Quartzite.|
24522|Tidnamurkuna Volcanics|65390|5|Briefly described|p13, p22 Fig. 3|Statherian|Statherian|Of Peake Metamorphics, Gawler Craton. Amygdaloidal basalts and acid volcanics. A rhyolite within this unit has a SHRIMP U-Pb zircon age of 1780 +/- 12 Ma.||||||
24522|Tidnamurkuna Volcanics|66302|5|Briefly described|p28, p30, p33, p63|Statherian|Statherian|Peake and Denison Domain, Gawler Craton. Deposited in a shallow marine setting. Misspelt as the Tidnamurkana Volcanics on p30.  Possesses similar geochemistry to the Bottletree and Argylla Formations and the Eastern Creek Volcanics. Ages are derived from Fanning et al. (2007).|1781 +/- 8 Ma to 1789 +/- 10 Ma ||||Metamorphosed amygdaloidal basalt and porphyritic rhyolites with minor phyllite and marble.|
24522|Tidnamurkuna Volcanics|67181|5|Briefly described|p617, p629|Statherian|Statherian|Peake and Denison Inlier, Gawler Craton. Interlayered with the sediments of the Peake Metamorphics, rhyolites age of 1790-1770 Ma from Fanning et al. 2007|1790-1770 Ma, age of rhyolites|||||
24522|Tidnamurkuna Volcanics|67536|5|Briefly described|Map Legend|Statherian|Statherian|Gawler Craton.|ca. 1780 +/- 12 Ma; 1746 +/- 6 Ma.|Of Peake Metamorphics.|||Basalt and rhyolite.|02-APR-14
24522|Tidnamurkuna Volcanics|67581|6|Mentioned|p45|||Gawler Craton. Pre-Kimban (1790-1740 Ma) Orogeny.||||||
24522|Tidnamurkuna Volcanics|70721|6|Mentioned|p70|||Peake and Denison Inliers.|c. 1780 Ma|||||
24522|Tidnamurkuna Volcanics|70938|5|Briefly described|p807-809|Paleoproterozoic|Paleoproterozoic|Denison Range.|1806 +/- 27 Ma; Fanning et al. (1988).||||Basalt-dominated flows interrupted by rhyolitic volcanism.|
24522|Tidnamurkuna Volcanics|73298|6|Mentioned|p1073|Statherian|Statherian|Gawler Craton.|1774 Ma|||||
80056|Tietz Subsuite|70405|4|Described|p36|Paleoproterozoic|Paleoproterozoic||1710 Ma - 1720 Ma|Bumbumbie Suite|||Metabasalts are massive, fine grained, non amygdaloidal and lacking any sedimentary intercalations.|
38061|Tiger Supersequence|24336|5|Briefly described|p99 Fig.3|||Correlated to the Wigunda Formation.||||||
38061|Tiger Supersequence|61544|6|Mentioned|p367 Fig.3. |Santonian|Turonian|Ceduna Sub-basin. Accelerated subsidence.||||Overlies White Pointer Supersequence. Is overlain by Hammerhead Supersequence.||
38061|Tiger Supersequence|66578|6|Mentioned|pp1006-1007, p1010.|Late Cretaceous|Late Cretaceous|Ceduna Sub-Basin, Bight Basin.||||Overlies White Pointer Supersequence. Is overlain by Hammerhead Supersequence.||
38061|Tiger Supersequence|69297|5|Briefly described|p14 fig 2.4, p23|Santonian|Turonian|Eyre, Ceduna and Duntroon Sub-basins. Maximum thickness fo approximately 4500m. Good potential oil and gas source rocks confirmed by dredging. See also p25 fig 2.9, p41, p44-p46, p48, p58, p60.||||Overlies the White Pointer Supersequence. Unconformably overlain by the Wobbegong Supersequence.||
38061|Tiger Supersequence|70067|5|Briefly described|Ceduna: Fig.2; p2. Regional: Fig.2; p2-3|Santonian|Turonian|Bight Basin. Comprises Wigunda Formation. Marine shales are potential source rocks and form a regional seal. Deltaic and shallow marine sandstones are potential oil and gas reservoirs according to petroleum systems modelling.||||Overlies White Pointer Supersequence. Is overlain by Tiger Supersequence.|Marginal marine, deltaic and open marine sediments thickening markedly to the south.|
26944|Timboon Sandstone|12781|6|Mentioned|p386|Late Cretaceous|Late Cretaceous|Otway Basin. Maximum thickness 1590m.||Sherbrook Group.||Unconformably overlies Waarre Formation. Abuts Flaxman and Paaratte Formations. Is overlain unconformably by Pebble Point Formation.||
26944|Timboon Sandstone|12796|5|Briefly described|p460, p456 Fig. 2|Maastrichtian|Campanian|Of the Sherbrook Group. Overlies Paarratte Formation; interfingers with and overlain partially by Wiridjil Gravels; also overlain by Massacre Shale. Geological Province: Otway Basin. ||||||
26944|Timboon Sandstone|22470|5|Briefly described|p13 Fig. 17|Maastrichtian|Campanian|Of Sherbrook Group.||||||
26944|Timboon Sandstone|24314|5|Briefly described|p61 Fig.2||Turonian|Geological Province: Otway Basin. Max. Thickness 1590m. Of the Sherbrook Subgroup.||||||30-NOV-04
26944|Timboon Sandstone|24551|6|Mentioned|p245|||Of the Sherbrook Group.||||||
26944|Timboon Sandstone|24562|5|Briefly described|p3, 8|Late Cretaceous|Late Cretaceous|Of the Sherbrook Group.  Geological Province: Otway Basin.||||||
26944|Timboon Sandstone|42361|3|Fully described|p17|Turonian||||||||
26944|Timboon Sandstone|42545|6|Mentioned|p19|||Otway Basin||||||
26944|Timboon Sandstone|43195|5|Briefly described|Map Legend||Late Cretaceous|See also commentary on back of map. Of Sherbrook Group.||||||
26944|Timboon Sandstone|43219|5|Briefly described|Fig.3,p6.|Maastrichtian|Campanian|Of Sherbrook Group.||||||14-APR-08
26944|Timboon Sandstone|43733|6|Mentioned|Fig.2.11,p65||Late Cretaceous|||||||
26944|Timboon Sandstone|43814|6|Mentioned|Fig.3,p115|||||||||
26944|Timboon Sandstone|44133|4|Described|p147|Maastrichtian|Santonian|Of the Sherbrook Group. Geological Province: Otway Basin. Unconformably overlain by Dilwyn Formation. Thickness: 1590m. ||||||
26944|Timboon Sandstone|61017|5|Briefly described|p5 Fig. 2|Maastrichtian|Campanian|Of the Sherbrook Group. Geological Province: Otway Basin.||||||07-FEB-11
26944|Timboon Sandstone|61230|5|Briefly described|p319 Fig.2, p329. |Maastrichtian|Campanian|Delta front to delta plain progradational depositional settings.||Unit in Sherbrook Group.||Overlies Paaratte Formation.|Sandstone, mudstone; increasingly sandstone-dominated up-unit to coarse sandstone and conglomerate.|
26944|Timboon Sandstone|61470|5|Briefly described|p28 Fig. 5|Maastrichtian|Campanian|Of the Sherbrook Group. Overlies Skull Creek Formation; underlies Massacre Shale. Geological Province: Otway Basin.||||||12-OCT-05
26944|Timboon Sandstone|61547|6|Mentioned|p461 Fig.2, p462. |Maastrichtian|Turonian|||Unit in Sherbrook Group.||Overlies Waarre Sandstone. Is overlain by Pebble Point Formation.||
26944|Timboon Sandstone|61622|5|Briefly described|p436 Fig. 2|Cretaceous|Cretaceous|Sherbrook Group. Geological Province: Otway Basin.||||||07-FEB-11
26944|Timboon Sandstone|61623|6|Mentioned|p449 Fig. 4|Late Cretaceous|Late Cretaceous|Of Sherbrook Group. Geological Province: Otway Basin.||||||07-APR-09
26944|Timboon Sandstone|61625|5|Briefly described|p475, p476 Fig. 1, p477, p480, p483|Late Creatceous|Late Cretaceous|Of Sherbrook Group. Geological Province: Otway Basin. Fine to very corase-grained sandstones, lacks bioturbated horizons and contains leaf fossils.||||||07-FEB-11
26944|Timboon Sandstone|61626|5|Briefly described|p486, p486 Fig. 2|Late Cretaceous|Late Cretaceous|Of Sherbrook Group. Geological Province: Otway Basin.||||||07-APR-09
26944|Timboon Sandstone|61627|5|Briefly described|p500 Fig. 2|Late Cretaceous|Late Cretaceous|Of Sherbrook Group. Geological Province: Otway Basin.||||||07-FEB-11
26944|Timboon Sandstone|61628|5|Briefly described|p509 Fig. 3|Late Cretaceous|Late Cretaceous|Of Sherbrook Group. Geological Province: Otway Basin.||||||07-APR-09
26944|Timboon Sandstone|63122|5|Briefly described|p17 Fig. 4.3|Maastrichtian|Turonian|Of the Sherbrook Group. Max. thickness: 1590m. Geological Province: Otway Basin. ||||||
26944|Timboon Sandstone|63124|3|Fully described|p48 Fig. 5.1, p49 Fig. 5.2, p82-84|Maastrichtian|Santonian|Supersedes all former Timboon nomenclature, incl: T.Sst Mbr, T.Sand, Curdies Fm and C. Beds, T. Sand and T.Sand Member. Unconform.below Wangerrip Group. Max.thick:1590m. Geol.Prov: Otway Basin. Of Sherbrook Gp in SA; in VIC is upper member of Paaratte Fm.||||||
26944|Timboon Sandstone|63129|5|Briefly described|p137|||Geological Province: Otway Basin. Offshore, this unit passes laterally into the interbedded shale-sand facies of Paaratte Formation. ||||||
26944|Timboon Sandstone|63269|5|Briefly described|p605|Late Cretaceous|Late Cretaceous|Otway Basin.||Sherbrook Group.||||
26944|Timboon Sandstone|63431|5|Briefly described|p677 Fig. 2|Maastrictian|Turonian|Of the Sherbrook Group. Geological Province: Penola Trough/Otway Basin.||||||07-FEB-11
26944|Timboon Sandstone|66245|5|Briefly described|p6 Fig.5, p64 Fig.C6.|Maastrichtian|Campanian|The top of this unit is used to correlate well logs in this study.||Unit in Sherbrook Group.||Overlies Paaratte Formation.|Fluvial sandstones and floodplain claystones and some coals.|
26944|Timboon Sandstone|67061|6|Mentioned|p546 Fig.3.|Maastrichtian|Campanian|||Unit in Sherbrook Group.||Overlies Paaratte Formation.||15-MAR-12
26944|Timboon Sandstone|67366|5|Briefly described|p103 Fig.2. |Maastrichtian|Campanian|||Topmost unit in Sherbrook Group.||Overlies Paaratte Formation and Skull Creek Mudstone. Is unconformably overlain by Massacre Shale.|Marginal marine and lower coastal plain sandstone and mudstone.|
26944|Timboon Sandstone|67367|5|Briefly described|p131 Fig.2. |Maastrichtian|Campanian|||Unit in Sherbrook Group.||||
26944|Timboon Sandstone|69297|5|Briefly described|p79, p98|Maastrichtian|Campanian|Otway Basin. ||Sherbrook Group||Faulted against or overlies the Paaratte Formation. Overlain by the Massacre Shale, Wiridjil Gravel or the Pebble Point Formation.|Sandstone.|
26944|Timboon Sandstone|69651|5|Briefly described|p10, p33-34|Late Cretaceous|Late Cretaceous|Otway Basin. Intraformational mudstones may form seals.||Sherbrook Group.||Overlies Paaratte Formation. Is overlain unconformably by Eastern View Formation.|Sandstone, shale.|
26944|Timboon Sandstone|70077|5|Briefly described|Nelson: Fig.2; p2. Regional: Fig.4; p8|Maastrichtian|Campanian|Otway Basin. Mudstones within distal equivalents in the Nelson Sub-basin provide intraformational seals.||Sherbrook Group.||Overlies Paaratte Formation or Skull Creek Mudstone. Is overlain by Massacre Shale and Wiridjil Gravel.||
26944|Timboon Sandstone|70078|5|Briefly described|Northern: Fig.2. Regional: Fig.4|Maastrichtian|Campanian|Gambier Embayment and Voluta Trough.||Sherbrook Group.||Overlies Paaratte Formation. Is overlain by Massacre Shale.||
26944|Timboon Sandstone|70193|5|Briefly described|p284 Fig 2, p285 fig 3|Maastrichtian|Maastrichtian|Geological province: Otway Basin. I. korojonense dinocyst zone. Part of the Sherbrook Supersequence.||||Underlain conformably by the Paaratte Formation.||
26944|Timboon Sandstone|70880|6|Mentioned|p77|Maastrichtian|Campanian|Otway Basin.||||||
26944|Timboon Sandstone|71266|6|Mentioned|p614 Fig.3|Late Cretaceous|Late Cretaceous|Otway Basin.||||||
26944|Timboon Sandstone|73357|5|Briefly described|p23-24, p43, p45, p47|Maastrichtian|Campanian|Otway Basin. Lithostratigraphic boundary with Paaratte Formation can be uncertain. Correlated with Isabelidinium korojonense Dinocyst Zone, Forcipites longus Spore-Pollen Zone, and I. pellucidum Dinocyst Zone, marginal to nearshore marine setting. Upper part correlates with Manumiella druggii Dinocyst Zone, marginal to shelfal marine depositional environment.||Of Sherbrook Group.||Overlies Paaratte Formation, underlies K/Pg Boundary Shale|Predominantly sandy unit.|
26944|Timboon Sandstone|73383|4|Described|p3, p23, p119, p140, p247, p266-267|Maastrichtian|Campanian|Otway Basin. Lithologies based on geochemistry using the ChemLith classification also includes calcareous sandstone, limestone; and using the Herron classification (1988) includes quartz arenite, sublith-arenite, lith-arenite, Fe-sand, Fe-shale. See also p322.||Sherbrook Group||Overlies Paaratte Formation, underlies Wangerrip Group|Sandstones, mudstones.|
26944|Timboon Sandstone|73385|5|Briefly described|p5|Maastrichtian|Campanian|Otway Basin.||Sherbrook Group||Overlies Paaratte Formation, underlies Wangerrip Group.|Marginal marine and lower coastal plain sandstones, mudstones.|
26944|Timboon Sandstone|73386|4|Described|p4, p6, p10-12, Attachment A1|Maastrichtian|Campanian|Otway Basin. Changes facies from fluvial-upper delta plain onshore and nearshore, to lower delta plain, interdistributary sandstone and shale mid-shelf, and marine shale in the outer shelf. Occurs within the Lower Forcipites longus Spore-Pollen Subzone, late Campanian to Maastrichtian in age. Sharp boundary with overlying Cretaceous/Paleogene boundary shale.||Sherbrook Group||Overlies Paaratte Formation, underlies Wangerrip Group, Cretaceous/Paleogene boundary shale|Characterised by mainly white fine to very coarse sandstones with siltstone/mudstone interbeds.|
26944|Timboon Sandstone|73594|6|Mentioned|p4|Maastrichtian|Campanian|Otway Basin.||Sherbrook Group||Overlies Paaratte Formation||
26283|Tinchoo Formation|13497|3|Fully described|v, vi, viii, xii, p69 fig 6.1|Ladinian|Anisian|Cooper Basin. Originally defined by Powis (1989) who subdivided the unit into the Gilpeppee and Doonmulla Members in Queensland, however these members were not recognised in SA. Powis (1989) nominated one type section whilst Channon and Wood (1989) named another within the same well. Both authors also proposed seperate reference sections. Lithology in South Australia where it is thinned by erosion is also described. Maximum thickness of 109m in South Australuia. Petrography and lithology are discussed in some detail.  Interpreted to have been deposited in a low-sinuosity fluvial environment. Hosts oil in the James 1 well. Deposited by low-sinuosity river systems. Reservoir characteristics discussed. See also p104, p105, p110, p112-p114, p119, p157 tbl 10.1, p159, p161, p167, p170, p216.||Nappamerri Group|Includes the Gilpeppee and Doonmulla Members.|Conformably overlies the Arrabury Formation. Unconformably overlain by the Cuddapan Formation, Poolowanna Formation or Hutton Sandstone.  Equivalent to the Walkandi Formation.|Interbedded brown-grey siltstone and light grey sandstone (Doonmulla Member) overlain by uniform dense light grey to green siltstone with minor coal seams and conglomerate beds.|
26283|Tinchoo Formation|13516|5|Briefly described|p164, p171 fig 12|Middle Triassic|Middle Triassic|In Cooper, Eromanga Basins.|||Includes Doonmulla Member, Gilpepee Member.|||
26283|Tinchoo Formation|22839|6|Mentioned|P33||Early Triassic|||||||
26283|Tinchoo Formation|22883|6|Mentioned|P29|Late Triassic|Middle Triassic|||||||
26283|Tinchoo Formation|22924|6|Mentioned|49|||||||||
26283|Tinchoo Formation|23155|6|Mentioned|p23|Mesozoic|Mesozoic|The Tinchoo Formation forms part of the Nappamerri Group, however it is not preserved on STRZELECKI.||||||
26283|Tinchoo Formation|23375|4|Described|Fig2 p265, 293|Ladinian|Anisian|In the Cooper Basin.||||||17-JAN-08
26283|Tinchoo Formation|24210|5|Briefly described|p133 Fig. 2|Middle Triassic|Middle Triassic|Of the Nappamerri Group.  Geological Province: Cooper Basin.||||||
26283|Tinchoo Formation|24282|6|Mentioned|p11|||Cooper-Eromanga Basin.||||||
26283|Tinchoo Formation|24372|5|Briefly described|p21|Triassic|Triassic|Geological Province: Cooper Basin.||||||
26283|Tinchoo Formation|42008|2|Defined|p271|Carnian|Anisian|Of Nappamerri Group.||||||
26283|Tinchoo Formation|42085|6|Mentioned|Fig.2 P374|||||||||
26283|Tinchoo Formation|43628|6|Mentioned|Fig.13|||||||||
26283|Tinchoo Formation|43711|6|Mentioned|p19||Triassic|||||||
26283|Tinchoo Formation|44133|4|Described|p65 Fig. 8.3, 86, 96|Upper Triassic|Triassic|Of the Nappamerri Group. Geological Province: Cooper Basin. Includes: Doonmulla Member, Gilpeppee Member. Conformably overlies Wimma Sandstone Member. Overlain by the Cuddapan Formation.||||||17-JAN-08
26283|Tinchoo Formation|60386|6|Mentioned|p299|Late Triassic|Early Triassic|Cooper/Eromanga Basin. Non-marine.||||||
26283|Tinchoo Formation|60717|5|Briefly described|p40 Fig. 2|Ladinian|Anisian|Of the Nappamerri Group. Overlies Arrabury Formation. Thickness: 100m. Geological province: Cooper Basin.||||||
26283|Tinchoo Formation|61015|6|Mentioned|p44|||||||||
26283|Tinchoo Formation|61613|5|Briefly described|p282 Fig. 2|Triassic|Early Triassic|Of Nappamerri Group. Includes Doonmulla and Gilpepee Members. Members. Underlain by Arrbury Formation. Geological Province: Cooper and Simpson Basins.||||||07-FEB-11
26283|Tinchoo Formation|61614|6|Mentioned|p290 Fig. 2|Middle Triassic|Early Triassic|Of Nappamerri Group. Geological Province: Cooper Basin.||||||17-MAR-09
26283|Tinchoo Formation|61615|6|Mentioned|p302 Fig. 2|Late Triassic|Middle Triassic|Of Nappamerri Group. Geological Province: Cooper Basin.||||||07-FEB-11
26283|Tinchoo Formation|61616|6|Mentioned|p330 Fig. 2|Early Triassic|Early Triassic|Of Nappamerri Group. Geological Province: Cooper Basin.||||||31-MAR-09
26283|Tinchoo Formation|62537|6|Mentioned|p191 Fig.2. |||Cooper Basin.||Unit in Nappamerri Group.||||
26283|Tinchoo Formation|62730|5|Briefly described|p352 Fig. 1|Late Triassic|Middle Triassic|Of the Nappamerri Group. Geological Province: Cooper Basin.||||||21-APR-08
26283|Tinchoo Formation|63978|2|Defined|p23, Fig. 3|Middle Triassic|Middle Triassic|Top of Nappamerri Gp. Unconformable on Arrabury Fm.; unconformable below Cuddapan Fm. Thickness: 263m. Interbedded sandstone, siltstone, mudstone, minor coal; sandstone is dominant in lower part, siltstone/mudstone/minor coal dominates upper section.||||||07-FEB-11
26283|Tinchoo Formation|64048|5|Briefly described|p64 Tb. 2|||Top unit of Nappamerri Group. Unconformable on Arrabury Formation. Geol.Prov: Cooper Basin. Comprises a fining-upwards succession with lower sublabile to quartzose fluvial sandstones (Doonmulla Member) and an upper sandstone-dominated Gilpeppee Member.||||||07-FEB-11
26283|Tinchoo Formation|64197|6|Mentioned|p625 Fig.1c|Middle Triassic|Middle Triassic|Cooper Basin. Underlies the Nappamerri Unconformity.||Unit in Nappamerri Group.||Overlies Wimma [Sandstone] Member (Arrabury Formation).||
26283|Tinchoo Formation|64665|5|Briefly described|p53 Fig.2.|Middle Triassic|Middle Triassic|Cooper Basin.|||Includes Doonmulla and Gilpeppee Members.|Overlies Arrabury Formation.||
26283|Tinchoo Formation|65238|5|Briefly described|p9|||Unconformably overlies the Arrabury Formation.||||||17-FEB-10
26283|Tinchoo Formation|65489|5|Briefly described|p15, p48-49, p55, p63, p96, p131, p150|Late Triassic|Middle Triassic|Cooper Basin. 100m thick. Oil reservoir accounting for 3% of the Basin's production.||Unit in Nappamerri Group.|Includes Gilpeppee and Doonmulla Members.|Overlies Arrabury Formation. May correlate with Peera Peera Formation.||
26283|Tinchoo Formation|67402|6|Mentioned|p90, p90 fig CPR4|||||Nappamerri Group|Includes the Doonmulla Member and Gilpeppee Member.|Unconformably overlies the Arrabury Formation.||
26283|Tinchoo Formation|68731|5|Briefly described|p200 Fig 3.110, p207, p208|Ladinian|Anisian|Powis (1989). Cooper Basin. ~ 125-200 m thick. Lower: highly sinuous fluvial environment. Upper: extensive fluvio-lacustrine environment. Palynofloras indicate Anisian-Ladinian (Gray and McKellar 2002).||Of the Nappamerri Group.|Includes the Doonmulla Member and the Gilpeppee Member.|Unconformably underlain by the Wimma Sandstone Member and the Arrabury Formation. Unconformably overlain by the Cuddapan Formation, and the Poolowanna Formation, or the Hutton Sandstone.|Comprises interbedded sandstone, silstone, mudstone and minor coal, with sandstone dominant in the lower part and siltstone, mudstone, and minor coal in its upper part.|
26283|Tinchoo Formation|69454|5|Briefly described|p38:4, 9|Ladinian|Anisian|Cooper Basin.||Nappamerri Group.||Uppermost part may be equivalent to Peera Peera Formation (Pedirka Basin).||12-JUL-16
26283|Tinchoo Formation|69594|5|Briefly described|p524|||Cooper Basin.||||Is overlain unconformably by Poolowanna Formation.||
26283|Tinchoo Formation|69673|6|Mentioned|p153 fig 125|||||Nappamerri Group||Overlies Arrabury Formation||
26283|Tinchoo Formation|69728|6|Mentioned|p285|||Cooper Basin.||Nappamerri Group.||||
26283|Tinchoo Formation|69797|5|Briefly described|p17 Fig.2, p18|Late Triassic|Middle Triassic|Oil reservoir. Age: Anisian - Carnian (approximated from figure). Geol. Prov: Cooper Basin. Presented in figure as Tinchoo Fm.||Nappamerri Group|||Oil reservoir.|
26283|Tinchoo Formation|69946|5|Briefly described|p9, p36, p54|Late Triassic|Middle Triassic|Cooper Basin.||Unit in Nappamerri Group.|Includes Doonmulla and Gilpeppee Members.|Conformably overlies Arrabury Formation. Is overlain unconformably by Cuddapan Formation.||
26283|Tinchoo Formation|69947|5|Briefly described|p13 Fig.7.2|Middle Triassic|Middle Triassic|Cooper Basin.||Nappamerri Group.||||
26283|Tinchoo Formation|70317|6|Mentioned|p33|Middle Triassic|Middle Triassic|Cooper Basin.||Nappamerri Group.||Overlies Wimma Sandstone Member (Arrabury Formation). Is overlain unconformably by Cuddapan Formation.||
26283|Tinchoo Formation|70823|4|Described|iv, p40, p75-p79, p82|Middle Triassic|Middle Triassic|Cooper Basin. Deposited in sinuous meandering streams or fluviolacustrine environments. A maximum of 109m thickness is preserved in South Australia and a maximum 263m in Queensland. Outcrop and palynological characteristics are discussed.||Nappamerri Group|Includes the Gilpepee and Doonmulla members.|Conformably overlies the Wimma Sandstone Member (of the Arrabury Formation). Unconformably overlain by the Morney beds and Cuddapan Formation.|Planar cross-bedded, fine to medium grained sandstone with thin siltstone interbeds.|
26283|Tinchoo Formation|70824|5|Briefly described|p7, p9, p104|Ladinian|Anisian|Cooper Basin. Up to 109m thick. Deposited as sinuous meandering streams or fluviolacustrine environments.||Nappamerri Group|Includes the Doonmulla Member and the Gilpeppee Member.|Overlies the Wimma Sandstone Member (Arrabury Formation). Unconformably overlain by the Morney beds and Cuddapan Formation.||
26283|Tinchoo Formation|70946|5|Briefly described|p1089|Middle Triassic|Middle Triassic|Cooper Basin. Deposited in a sinuous meandering stream fluvio-lacustrine environment.||Nappamerri Group.||Overlies the Arrabury Formation. Unconformably overlain by the Cuddapan Formation.||08-OCT-18
26283|Tinchoo Formation|71342|6|Mentioned|Ch5 p9, Ch5 p36, Ch5 p54|Carnian|Anisian|Cooper Basin. Palynological zone is given in fig 5.3 Ch5 p36. Deposited in Sinuous meandering streams or fluvio-lacustrine environments. See also  Ch7 p13, Ch13 p4, Ch13 p7-p8, Ch13 p36.||Nappamerri Group|Includes the Doonmulla Member and the Gilpeppee Member.|Overlies the Toolachee Formation. Overlies the Arrabury Formation. Unconformably overlain by the Cuddapan Formation.||
26283|Tinchoo Formation|73167|6|Mentioned|p664 Fig. 2|Triassic|Triassic|Cooper Basin.||Nappamerri Group||||
26283|Tinchoo Formation|73244|6|Mentioned|p86|Triassic|Triassic|Cooper Basin.  Along with Callamurra Member, Panning Member and Wimma Sandstone Member , shown as floodplain, lacustrine, fluvial channels.||||||
26283|Tinchoo Formation|73251|6|Mentioned|p62|Middle Triassic|Middle Triassic|Cooper Basin. Sinuous meandering streams and fluviolacustrine depositional environments. Hydrocarbon source rock that contains[?] oil.||Nappamerri Group||Underlain by Arrabury Formation including Wimma Sandstone Member.||
26283|Tinchoo Formation|73343|6|Mentioned|p337|Triassic|Triassic|Cooper Basin.||Nappamerri Group||Underlain by Wimma Sandstone Member.||
26283|Tinchoo Formation|73479|5|Briefly described|p156 Fig.2, p159|Triassic|Triassic|Cooper Basin. Floodplain, lacustrine, fluvial channels depositional environment. Major regional unconformity separates the overlying Eromagma Basin.|ca 238 Ma|Nappamerri Group||Overlies Wimma Sandstone Member, unconformably underlies Cuddapan Formation||
27241|Tingana Clay|23154|5|Briefly described|Map Legend|Holocene|Holocene|Geological Province - Lake Eyre Basin - Callabonna Basin.||||||
27241|Tingana Clay|23155|5|Briefly described|p37|||This unit is the sticky grey clay recorded along the banks of Strzelecki Creek.  No suitable type section has been located.||||||
27241|Tingana Clay|23478|5|Briefly described|p28|Holocene|Pleistocene|||||||
27241|Tingana Clay|30749|2|Defined|p1|late Pleistocene|late Pleistocene|See also p2. Prob.Late Pleistocene||||||14-NOV-14
27241|Tingana Clay|30804|6|Mentioned|p15|||On Table 1||||||
27241|Tingana Clay|30919|6|Mentioned|Map legend|Quaternary|Quaternary|||||||
27241|Tingana Clay|30921|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
27241|Tingana Clay|33820|6|Mentioned|Map legend|Quaternary|Quaternary|||||||
27241|Tingana Clay|33821|6|Mentioned|Map legend|Recent|Pleistocene|Pleistocene - Recent||||||
27241|Tingana Clay|33822|6|Mentioned|Map legend|Quaternary|Quaternary|||||||
27241|Tingana Clay|33823|6|Mentioned|Map legend|Quaternary|Quaternary|||||||
27241|Tingana Clay|33824|6|Mentioned|Table 2|||||||||
27241|Tingana Clay|33827|6|Mentioned|Table 1|||||||||
27241|Tingana Clay|33828|6|Mentioned|Table 1|||||||||
27241|Tingana Clay|38068|6|Mentioned|p78|||||||||
27241|Tingana Clay|42543|5|Briefly described|p4|||||||||
27241|Tingana Clay|68068|5|Briefly described|Map legend|Holocene|Holocene|Callabonna Sub-basin, Lake Eyre Basin. Floodplain and channel deposits associated with Strzelecki Creek; equivalent in  Callabonna Creek. Interbedded with longitudinal dunes around floodplain margins. Aboriginal fire-hearths within the top. |8 ky to present.||||Dark to pale grey clay with fine sand or clay pellets.|
27241|Tingana Clay|69023|5|Briefly described|p130, p141|Holocene|Holocene|Of Firman (1970). Exposed along the floor of Strzelecki Creek. Flood-channel and overbank deposits incorporating aeolian and fluvially reworked aeolian dune sands of several ages. Variable thickness from <1m to ~2.5m.|>8000- <3000 yB.P.||||Pale grey to light olive-grey structured clay, with fine sand consisting of quartz grains and clay pellets; interbedded with longitudinal dunes around floodplain margins.|
79273|Tip Top Granite|70659|5|Briefly described|p4, p9-10|Palaeoproterozoic|Palaeoproterozoic|Part of basement to the Spencer Domain. Kimban Orogeny (1730-1690 Ma) tectonic fabrics were folded by (~1620-1570 Ma) Kararan Orogeny.||||Intrudes Broadview Schist.|Medium- to very coarse-grained quartz-K feldspar-plagioclase-muscovite +/- tourmaline granitic gneiss.|
79273|Tip Top Granite|70721|2|Defined|p63-p70, p72-p75|Paleoproterozoic|Paleoproterozoic|Spencer Domain, Gawler Craton. Named for the Tip Top Dam, Katunga Station (710715mE, 6360590mN, GDA 94, zone 53). The type locality is defined as the area extending for 200m around the point 716640 mE, 6358730mN (GDA 94, zone 53). A reference locality is located along Iron Knob- Whyalla railway siding ~30km northwest of Whyalla. Time equivalent to the Wertigo Granite. Outcrop extends over an area ~25km north-south by 10km east-west between Tip Top and Upper Nine Mile dams on Katunga, Roopena and Pandurra stations. Previously classified as an unnamed part of the Lincoln Complex. Petrography, deformational fabrics, geochemistry and geochronology are discussed in detail.|1773 +/- 6 Ma SHRIMP zircon (present study)|||Intrudes the Broadview Schist.|Orange to pink, medium to very coarse-grained, equigranular to megacrystic granite.|
79273|Tip Top Granite|70816|5|Briefly described|p3-4|Statherian|Statherian|Gawler Ranges region. Underwent LT metamorphism during 1730-1690 Ma Kimban Orogeny.|~1775 Ma|||||
79273|Tip Top Granite|70948|5|Briefly described|p974-975|Statherian|Statherian|Geological province: Gawler Craton.|ca. 1775 Ma|||In faulted contact with Cooyerdoo Granite. Underwent LT metamorphism during 1730-1690 Ma Kimban Orogeny.||
79273|Tip Top Granite|71037|5|Briefly described|p21 Fig.1, p22-23 Fig.2, p24|Paleoproterozoic|Paleoproterozoic|U-Pb SHRIMP Age 1773 +/- 6 Ma (McAvaney et al., 2016). See also p26-27, p27 Fig.6.|1773 +/- 6 Ma|||Intrudes Broadview Schist at time of deformation. Shown as younger than Wire Dam Dolerite and older than Moonabie Formation.|Granite, gneissic, coarse-grained to pegmatitic, quartz-feldspar-muscovite, garnet and tourmaline.|
79273|Tip Top Granite|71129|4|Described|p1,18,21,24,26,28-30,46,177|Statherian|Statherian|Geological Province: Spencer Domain, Gawler Craton. Exposed as low broad hills with small discontinuous platform exposures and broad areas of subcrop in close association with Broadview Schist. Contact with Broadview Schist is broadly parallel to tectonic fabric deforming both units i.e. syn-tectonic, local sheet injection along foliation. Deformation and tectonic fabric interpreted to have been formed at c. 1775 Ma, coeval with Tip Top Granite emplacement. Cut by Pankalla Fault via dextral movement. Peraluminous, LREE enriched and isotopically evolved signature indicate derivation from partial melting of a sedimentary protolith. Inherited zircon peaks indicate similarities to the detrital zircon spectra of Broadview Schist, therefore suggestive of a partial melting of a Broadview Schist sedimentary succession-equivalent in the lower crust. See also p184,189,199,204-205,225,227.|c. 1773+\-6 Ma (SHRIMP U-Pb, magmatic xtal)|||Intruded into, and interleaved with Broadview Schist.|Orange to pink medium- to very coarse-grained equigranular to megacrystic S-type granite; quartz, K-feldspar, plagioclase and muscovite with minor tourmaline and trace zircon.|
79273|Tip Top Granite|71130|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Age from (McAvaney et al., 2016).|1773 +/- 6 Ma SHRIMP U-Pb||||Granite, gneissic, coarse-grained to pegmatitic, quartz-feldspar-muscovite +/- garnet +/- tourmaline.|
79273|Tip Top Granite|71131|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Age derived from (McAvaney et al, 2016).|1773 +/- 6 Ma SHRIMP U-Pb||||Granite, gneissic, coarse-grained to pegmatitic, quartz-feldspar-muscovite +/- garnet +/- tourmaline.|
79273|Tip Top Granite|71317|5|Briefly described|p16|Palaeoproterozoic|Palaeoproterozoic|Spencer Domain, Gawler Craton.|c. 1775 Ma|||||
79273|Tip Top Granite|71414|6|Mentioned|p42 Fig 1, p43|Statherian|Statherian|Geological province: Gawler Craton.|~1770 Ma|||Intrudes Broadview Schist.||
79273|Tip Top Granite|71559|6|Mentioned|p15 Fig 1|Paleoproterozoic|Paleoproterozoic|Geological province: Gawler Craton.||||||
79273|Tip Top Granite|71859|5|Briefly described|p2, p4, p6|Statherian|Statherian|Spencer Domain, southern Gawler Craton.|c. 1775 Ma|||||
79273|Tip Top Granite|71862|6|Mentioned|p2, p8, p12|Paleoproterozoic|Paleoproterozoic||c. 1775 Ma|||||
79273|Tip Top Granite|72058|6|Mentioned|p172|||Middleback Ranges, Gawler Craton.|~1790-1770 Ma|||||
79273|Tip Top Granite|72089|6|Mentioned|p3|Palaeoproterozoic|Palaeoproterozoic|Gawler Craton.||||||
79273|Tip Top Granite|72090|6|Mentioned|p10|Statherian|Statherian|Spencer Domain, Gawler Craton.|c. 1775 Ma|||||
79273|Tip Top Granite|72237|6|Mentioned|p29|Paleoproterozoic|Paleoproterozoic|Geological province: Gawler Craton.||||||
79273|Tip Top Granite|72463|6|Mentioned|p2|Paleoproterozoic|Paleoproterozoic|||||||
79273|Tip Top Granite|72484|5|Briefly described|p22|||Immediately E of Middleback Ranges, Gawler Craton. Contains zircons inherited from the 2823 +/- 37 Ma protolith of Coolanie Gneiss.|~1775 Ma.|||||
79273|Tip Top Granite|73110|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic||||||Granite, gneissic, coarse-grained to pegmatitic, quartz-feldspar-muscovite +/- garnet +/- tourmaline.|
79273|Tip Top Granite|73130|6|Mentioned|[poster] Fig 1|Paleoproterozoic|Paleoproterozoic|||||||28-OCT-22
79273|Tip Top Granite|73234|6|Mentioned|p19|Statherian|Statherian||c. 1775 Ma|||||
79273|Tip Top Granite|73525|5|Briefly described|p19 Fig.13|Statherian|Statherian|Spencer Domain.|~1770 Ma crystallisation age||||Felsic intrusive.|
29838|Tommie Wattie Formation|22884|2|Defined|p40 Fig. 1, p41||Paleoproterozoic|Of the Thackaringa Group. Correlates with Cues Formation. Overlain by Weekeroo Formation. Max. thickness: 2000m. Historical information regarding previous informal nomenclature included.||||||26-MAR-09
29838|Tommie Wattie Formation|62592|6|Mentioned|p14. |||Olary Domain, Curnamona Province.||||||
29838|Tommie Wattie Formation|62993|5|Briefly described|p2, p4, p8, p37, p38, p39, 40|Paleoproterozoic|Paleoproterozoic|Olary Domain.|~1718 Ma|Wiperaminga Subgroup||Overlain by Peryhumuck Formation, Ethiudna Subgroup, Overlies George Mine Formation|Andalusite rich pelites.|19-DEC-21
29838|Tommie Wattie Formation|63102|4|Described|p14-19,34|||Geological province: Olary Domain, Curnamona Province. Type locality: NW of Tommie Wattie Bore, exposed ~1.7km thick sequence of mixed fine-grained schistose psammopelite and psammite (Laing 1996b). Reference localities occur at the Tommie Wattie Bore area of the Outalpa Inlier; the Northern Walparuta Inlier both south and north of the antiformal axis. Non-albitised metasediment-dominated assemblage (Laing 1996b). Thick, fining-upwards metasedimentary succession, and is best known in the northern Walparuta and Bimbowrie inliers. Possibly stratigraphically equivalent to George Mine Formation (Laing 1996b); or lowermost part of the Ethiudna Subgroup (Flint 2001).||Unit of Wiperaminga Subgroup.||Overalin by Peryhumuck Formation. Equivalent to Thackaringa Group, Thorndale Composite Gneiss, Clevedale Migmatite. Similar stratigraphically position to Mooleugore Formation.|Bedded schists, mica schists and andalusite schists.|22-OCT-19
29838|Tommie Wattie Formation|64741|5|Briefly described|p301 Fig. 4|Paleoproterozoic|Paleoproterozoic|Of Wiperaminga Subgroup (Curnamoma Group). Overlies George Mine Fm. Thickness: 1.5km. Geological province: Olary Domain. Lower interbedded psammite and psammopelite, fining upwards into andalusite-rich pelite.||||||07-FEB-11
29838|Tommie Wattie Formation|64944|4|Described|p27, p28 Fig. 1, p29 Tb. 1|Paleoproterozoic|Paleoproterozoic|Of Wiperaminga Subgroup (Curnamona Group). Age: ~1718ma. Thick upward-fining package from psammites, showing sedimentary structures, to andalusite pelite; volcanic interbeds (Abminga Subsuite).||||||07-FEB-11
29838|Tommie Wattie Formation|66302|5|Briefly described|p36 Fig.9, p37, p39|Statherian|Statherian|Olary Domain, Curnamona Province. |ca. 1718 Ma|Wiperaminga Subgroup||Overlies the George Mine Formation.||
29838|Tommie Wattie Formation|67540|5|Briefly described|p29 Tb.2|Paleoproterozoic|Paleoproterozoic|||Of the Willyama Supergroup.||Intruded by the Triangle Hill Granite.||03-FEB-16
29838|Tommie Wattie Formation|69650|5|Briefly described|p5, p19|||Both references refer to this unit being of the lower Willyama Supergroup Granite [?].||Unit in Willyama Supergroup.||Intruded by Triangle Hill Granite.|Metasediments.|
29838|Tommie Wattie Formation|70405|4|Described|p9 table 1, p18, p19, p25, p43 Table 3, |Paleoproterozoic|Paleoproterozoic|Incorrectly named Whey Whey Schist in previous study. Seven informal mapping units have been distinguished.|1710 Ma-1720 Ma|Ethiunda Subgroup||Underlies Peryhumuck Formation, Toraminga Formation|Metasandstone with well preserved, shallow water sedimentary structures. Psammopelitic, pelitic schists, fine grained psammite and minor feldspathic calc-silicates interbedded with thin volcaniclastic psammite bands; volcaniclastic metasediments.|
29838|Tommie Wattie Formation|70657|3|Fully described|p10 Fig.4, p14-15, p17-23, p25, p29, p41|Statherian|Statherian|Laing (1996) after Grady et al. (1989). Type locality is immediately NW of Tommie Wattie Bore; outcrop described. Three reference localities described. Curnamona Province; Olary Domain. Restricted to the Outalpa Subdomain. Age inferred from Fig.4. No equivalent in Broken Hill Domain. Lateral relationship with Mooleugore Formation unknown. Distinguished from George Mine Formation in being non- or barely-migmatised and containing few or no albitite granofels layers.|~1720-1715 Ma.|Wiperaminga Subgroup|Outalpa Quartzite Member.|Equivalent to, overlies and faulted against George Mine Formation. Underlies transitionally the Peryhumuck Formation (Ethiudna Subgroup).|2.5 km thick upwards-fining succession, from psammite to andalusite pelite. Dark grey to brown psammopelites; clean pale brown metasandstones. Sedimentary structures spectacularly preserved locally.|
29838|Tommie Wattie Formation|70658|5|Briefly described|p3, 5-6, 8-9, 11-12, 15-16, 21, 23|Paleoproterozoic|Paleoproterozoic|See also p27-29, 39, 42. Olary Domain, Curnamona Province. Deposited in half-grabens from eroding adjacent horsts of George Mine Formation.|1718 Ma.|Ethiudna Subgroup.||Is overlain gradationally by Toraminga Formation. Is intruded by Abminga Subsuite.|Psammitic, chemical metasediments, including a highly deformed metaconglomerate; andalusite-pelite typical of upper part, grades into quartz-muscovite schist; alkali-feldspar alteration. Metabasalt.|
79176|Toolgana Supersuite|70831|5|Briefly described|p25-p26|Statherian|Statherian|Coompana Province.|c. 1613-1604 Ma|||||
79176|Toolgana Supersuite|71143|5|Briefly described|p427,429,431-432,435-437,440|Statherian|Statherian|Geological province: Coompana Province. Oldest rocks in the Eucla basement region. Contains chemical and isotopic characteristics of primitive arc rock. Calc-alkaline suite; geochemical analysis indicate a subduction origin or re-melting of a subduction-derived source, or incorporation of crustal material into a mantle-derived melt. No known rocks equivalent in age to the Toolgana Supersuite in the Madura Province.|c. 1610 Ma||||Foliated feldspar-porphyritic granites interleaved with medium-grained monzodiorite and rare monzogabbro.|
79176|Toolgana Supersuite|71165|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Eastern Coompana Province.|c.1613 Ma.||||Granitic and mafic gneiss.|
79176|Toolgana Supersuite|71169|5|Briefly described|p77|Statherian|Statherian|Coompana Province. Features arc-like geochemistry (Smithies et al., 2015b).|1613-1604 Ma (Wingate et al., 2015)||||Calc-alkaline granitic gneiss.|
79176|Toolgana Supersuite|71618|6|Mentioned|p133|Statherian|Statherian|Geological province: Coompana Province. Possible source of c~1500-1800 Ma detrital zircons in the Madura Formation, Loongana Formation and Decoration Sandstone.|c. 1610 Ma||||Granites and monzogranite.|
79176|Toolgana Supersuite|71891|5|Briefly described|p7, p30, p33-p34|||Coompana Province. See also p38-p40, p47, p49, p51-p52, p55.|c. 1610 Ma||||Migmatitic monzodioritic to granodioritic to monzogranitic gneiss and metadolerites.|
79176|Toolgana Supersuite|72242|5|Briefly described|p27,29-30|Calymmian|Statherian|Geological province: Musgrave Province. Associated with Kararan Orogeny. Coeval with Hiltaba Suite and Birksgate Complex, and extensive oceanic crust formation.|||Includes Koomalboogurra Suite.|||
79176|Toolgana Supersuite|72344|6|Mentioned|p3, p5, p7-p9, p16-p17, p28|Statherian|Statherian|Coompana Province. The same age as, and geochemically and isotopically similar to the St Peter Suite. Previously identified in drillcore from the Forrest Zone and Kutjara 1. Granites of this supersuite have protolith ages of c. 1591-1613 Ma. A magmatic age of 1614 +/- 12 Ma is derived via SHRIMP. Basement in CDP001 is assigned to this unit. Petrography, SHRIMP analyses and geochemistry are discussed for several samples. See also p96, p98, p102, p143, p169.|c. 1610-1620 Ma||Includes the Koomalboogurra Suite|Time equivalent of the St Peter Suite and Birksgate Complex.||04-SEP-19
79176|Toolgana Supersuite|72465|5|Briefly described|p4, 10, 17|||Spaggiari and Smithies (2015). Coompana Province. Product of arc magmatism and recycling of oceanic crust. Metamorphic ages range from 1179 +/- 10 Ma to 1150 +/- 10 Ma. Is similar geochemically, isotopically and in age to the St Peter Suite (western Gawler Craton). Basement lithologies described in detail; photos of core.|1613 +/- 13 Ma to 1591 +/- 11 Ma.|||Is overlain by Madura Formation.|Locally migmatitic monzodioritic to granodioritic to monzogranitic gneisses and metadolerites that have been metamorphosed to amphibolite facies.|
79176|Toolgana Supersuite|72466|5|Briefly described|p4, 10|||Spaggiari and Smithies (2015). Basement to Coompana Province. Metamorphosed between 1179 +/- 10 Ma and 1150 +/- 10 Ma. Derived from a mantle wedge or subduction-modified lithosphere. Has the same age, and similar geochemistry and isotopes, as St Peter Suite in western Gawler Craton.|1613/- 13 Ma to 1591 +/- 11 Ma.||||Locally migmatitic monzodioritic to granodioritic to monzogranitic gneisses and metadolerites that have been metamorphosed to amphibolite facies.|
79176|Toolgana Supersuite|72467|5|Briefly described|p4, 10|||Spaggiari and Smithies (2015). Coompana Province. Product of arc magmatism and recycling of oceanic crust. Metamorphic ages range from 1179 +/- 10 Ma to 1150 +/- 10 Ma. Is similar geochemically, isotopically and in age to the St Peter Suite (western Gawler Craton). Basement lithologies described in detail; photos of core.|1613/- 13 Ma to 1591 +/- 11 Ma.|||Is overlain by Madura Formation.|Locally migmatitic monzodioritic to granodioritic to monzogranitic gneisses and metadolerites that have been metamorphosed to amphibolite facies.|
79176|Toolgana Supersuite|72468|5|Briefly described|p4, p10, p13, p17|Statherian|Statherian|Coompana Province. Represents arc magmatism and recycling of oceanic crust. Same age as, and is geochemically and isotopically similar to St Peter Suite. Magmatic ages include 1613 +/- 4 Ma, 1611 +/- 7 Ma, 1613 +/- 13 Ma, 1604 +/- 6 Ma, and 1591 +/- 11 Ma. Metamorphic ages include 1179 +/- 10 Ma, 1150 +/- 10 Ma, and 1167 +/- 7 Ma.|c. 1610 Ma||||Granitic to monzodioritic rocks including locally migmatitic monzodioritic to granodioritic to monzogranitic gneisses and metadolerites that have been metamorphosed to amphibolite facies.|
79176|Toolgana Supersuite|72469|5|Briefly described|p4, p10|Statherian|Statherian|Coompana Province. Represents arc magmatism and recycling of oceanic crust. Same age as, and is geochemically and isotopically similar to St Peter Suite. Magmatic ages include 1613 +/- 4 Ma, 1611 +/- 7 Ma, 1613 +/- 13 Ma, 1604 +/- 6 Ma, and 1591 +/- 11 Ma. Metamorphic ages include 1179 +/- 10 Ma, 1150 +/- 10 Ma, and 1167 +/- 7 Ma.|c. 1610 Ma||||Granitic to monzodioritic rocks including locally migmatitic monzodioritic to granodioritic to monzogranitic gneisses and metadolerites that have been metamorphosed to amphibolite facies.|
79176|Toolgana Supersuite|72470|5|Briefly described|p4, p10, p13, p18|Statherian|Statherian|Coompana Province. Represents arc magmatism and recycling of oceanic crust. Same age as, and is geochemically and isotopically similar to St Peter Suite. Magmatic ages include 1613 +/- 4 Ma, 1611 +/- 7 Ma, 1613 +/- 13 Ma, 1604 +/- 6 Ma, and 1591 +/- 11 Ma. Metamorphic ages include 1179 +/- 10 Ma, 1150 +/- 10 Ma, and 1167 +/- 7 Ma.|c. 1610 Ma||||Granitic to monzodioritic rocks including locally migmatitic monzodioritic to granodioritic to monzogranitic gneisses and metadolerites that have been metamorphosed to amphibolite facies.|
79176|Toolgana Supersuite|72471|5|Briefly described|p4, p10|Statherian|Statherian|Coompana Province. Represents arc magmatism and recycling of oceanic crust. Same age as, and is geochemically and isotopically similar to St Peter Suite. Magmatic ages include 1613 +/- 4 Ma, 1611 +/- 7 Ma, 1613 +/- 13 Ma, 1604 +/- 6 Ma, and 1591 +/- 11 Ma. Metamorphic ages include 1179 +/- 10 Ma, 1150 +/- 10 Ma, and 1167 +/- 7 Ma.|c. 1610 Ma||||Granitic to monzodioritic rocks including locally migmatitic monzodioritic to granodioritic to monzogranitic gneisses and metadolerites that have been metamorphosed to amphibolite facies.|
79176|Toolgana Supersuite|72472|5|Briefly described|p4, p10|Statherian|Statherian|Coompana Province. Represents arc magmatism and recycling of oceanic crust. Same age as, and is geochemically and isotopically similar to St Peter Suite. Magmatic ages include 1613 +/- 4 Ma, 1611 +/- 7 Ma, 1613 +/- 13 Ma, 1604 +/- 6 Ma, and 1591 +/- 11 Ma. Metamorphic ages include 1179 +/- 10 Ma, 1150 +/- 10 Ma, and 1167 +/- 7 Ma.|c. 1610 Ma||||Granitic to monzodioritic rocks including locally migmatitic monzodioritic to granodioritic to monzogranitic gneisses and metadolerites that have been metamorphosed to amphibolite facies.|
79176|Toolgana Supersuite|72934|5|Briefly described|p2, p4, p11-12, App.A|Statherian|Statherian|Interpreted to be derived from a subduction-enriched mantle source, compatible with a primitive arc setting. Yielded U-Pb SIMS zircon magmatic crystallisation ages of 1618 +/- 6 Ma and 1618 +/- 9 Ma; a metamorphic age of 1163 +/- 8 Ma; and an inheritance age of c. 1720 Ma.|c. 1610 Ma||||Magnesian, calc-alkalic, high-K granitic to dioritic gneisses.|
79176|Toolgana Supersuite|72947|5|Briefly described|p4, p7-9, p12|Calymmian|Statherian|Coompana Province. Represents arc magmatism.|c. 1610 Ma / 1622 - 1591 Ma||Koomalboogurra Suite|Sheared contact with Bunburra Suite.||29-NOV-22
79176|Toolgana Supersuite|73084|4|Described|p: 12, 15, 32, 34, 44-45, 69-70, 72...|Statherian|Statherian|Coompana Province. Biranup Orogeny. Oldest rocks sampled in the Coompana Province. Upper amphibolite to granulite facies. Most likely subduction related; intruded c. 1724 to 1671 Ma or older crust. May represent westward-migrating arcs. Possibly a regionally extensive, primitive arc-related suite, based also on similarities with the St Peter Suite, where subduction may have been directed towards the Gawler Craton margin. Metamorphism is dated at 1179 +/- 10, 1153 +/- 9 and 1151 +/- 6 Ma. Report includes lithologic/petrographic description, structural analysis, whole-rock geochemistry, geochronology, Sm-Nd, Lu-Hf. Also p: 100-116, ~123-129, ~133-137, 142.|1613-1604 Ma||Koomalboogurra Suite||Granite gneiss, and locally, diorite to amphibolite gneiss. Includes monzodiorite, granodiorite to monzogranite gneiss.|
79176|Toolgana Supersuite|73091|5|Briefly described|map legend|Mesoproterozoic|Mesoproterozoic||||Includes Koomalboogurra Suite.|||
79176|Toolgana Supersuite|73224|5|Briefly described|p42, p44|Statherian|Statherian|Coompana Province, central. Underwent high-temperature anatexis at c. 1179-1150 Ma.|c. 1618-1604 Ma|||||
79176|Toolgana Supersuite|73225|5|Briefly described|p2, 4, 10, 18, p22 Fig.10|||Coompana Province. East of the Mulyawarra Shear Zone. Arc-related rocks; underwent high-T metamorphism and anatexis c.1179-1150 Ma. Age range also given as 1613-1604 Ma.|1618-1604 Ma.||Koomalboogurra Suite.||Migmatites.|
79176|Toolgana Supersuite|73641|6|Mentioned|p4||||||Koomalboogurra Suite|||
34547|Top Mount Sandstone beds|22772|5|Briefly described|Table13.1|Cryogenian|Cryogenian|||||||
34547|Top Mount Sandstone beds|22857|5|Briefly described|Tb. 13.1 (insert p70-71)|Torrensian|Torrensian|Of the Emeroo Subgroup (Burra Group).||||||
34547|Top Mount Sandstone beds|24321|5|Briefly described|Map legend|Adelaidean|Adelaidean|Parent: Emeroo Subgroup||||||
34547|Top Mount Sandstone beds|66884|5|Briefly described|p39 Fig.2, p41 Fig.3|||Appears as Top Mount Sandstone in Fig.2. Thickness: up to 950m.||Emeroo Subgroup||Is overlain by Willawalpa Formation.|Quartz arenite (grey-tan, medium to coarse grained, medium bedded, ripple cross-laminations, desiccation cracks and lenticular bedding); interbedded with subordinate siltstone (dark grey, thinly laminated); rare dolostone and limestone (grey).|
34547|Top Mount Sandstone beds|72456|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Marree 1:250k map sheet.|||||Quartzite and sandstone, medium to coarse-grained, with interbedded finely laminated siltstone and grey dolomite and limestone. Ripple marks, mudcracks, lenticular bedding and wavy lamination.|14-JUN-22
75082|Toraminga Formation|62993|6|Mentioned|p37|Paleoproterozoic|Paleoproterozoic|Olary Domain.||Ethiudna Subgroup||||15-DEC-21
75082|Toraminga Formation|64741|5|Briefly described|p301 Fig. 4|Paleoproterozoic|Paleoproterozoic|Of Ethiudna Subgroup (Curnamona Group). Geological province: Olary Domain.||||||07-FEB-11
75082|Toraminga Formation|64944|5|Briefly described|p28 Fig. 1, p29 Tb. 1|Paleoproterozoic|Paleoproterozoic|Of Ethiudna Subgroup (Curnamona Group). Geological province: Olary Domain.||||||07-FEB-11
75082|Toraminga Formation|66302|5|Briefly described|p36 Fig.9, p37, p39|Statherian|Statherian|Olary Domain, Curnamona Province. ||Ethiudna Subgroup||Overlies the Mooleugore Formation. Overlain by the Peryhumuck Formation.||
75082|Toraminga Formation|70405|4|Described|p9 table 1, p21, p43 Table 3|Paleoproterozoic|Paleoproterozoic|||Ethiunda Subgroup|Includes Bewooloo Member|Underlies Peryhumuck Formation, overlies Tommie Wattie Formation|Psammopelitic metasediments with calc-silicate, alkali feldspar rich psammite and tuffaceous metasandstone interbeds.|
75082|Toraminga Formation|70657|4|Described|p14-15, p24, p26, p32|Statherian|Statherian|Curnamona Province; Olary Domain. No equivalent in Broken Hill Domain.|1718 +/- 3 Ma|Ethiudna Subgroup||Overlies Mooleugore and ?Bewooloo Formations. Underlies Peryhumuck Formation.|Fine-grained psammitic schist with alkali-feldspar-rich granofels, and calcsilicate units.|
75082|Toraminga Formation|70658|5|Briefly described|p3, 6, 9, 11-12, 15, 21, 23, 28-29, 32|Paleoproterozoic|Paleoproterozoic|Olary Domain, Curnamona Province.|1718 Ma.|Ethiudna Subgroup.|Montstephen Metabasalt Member.|Overlies Tommie Wattie Formation gradationally. Is overlain gradationally by Peryhumuck Formation.|Fine-grained bedded psammite and calc-silicate.|
68745|Tournefort Metadolerite|24508|5|Briefly described|p31 (photo)|||Mafic dykes.  Intrudes a granite of the Donington Suite. Geological Province: Gawler Craton.  See also Tournefort Metadolerite dykes.||||||23-DEC-09
68745|Tournefort Metadolerite|60958|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Undifferentiated dolerite, metadolerite and amphibolite dykes, with plagioclase, hornblende, clinopyroxene, biotite, sphene and opaques. Altered, occasionally foliated. ~1800Ma. Geological Province: Gawler Craton.||||||07-NOV-08
68745|Tournefort Metadolerite|61070|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Fine to coarse-grained massive black gabbroic and dolerite dykes. Minimum age: ~1810Ma (U-Pb Zircon). Geological Province: Gawler Craton.||||||12-JAN-10
68745|Tournefort Metadolerite|61121|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Undifferentiated dolerite, metadolerite and amphibolite dykes, with plagioclase, hornblende, clinopyroxene, biotite, sphene and opaques; altered, occasionally foliated; ophitic texture. Age: ~1800Ma. Geological Province: Gawler Craton.||||||07-NOV-08
68745|Tournefort Metadolerite|63398|5|Briefly described|p669|Paleoproterozoic|Paleoproterozoic|Age: ca 1812-1750Ma. Mafic rocks of the Tournefort Dyke Swarm.  ||||||07-NOV-08
68745|Tournefort Metadolerite|64282|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Geol Prov: Gawler Craton. Age: ~1800Ma. Intrudes Gleesons Landing Granite. Includes undiff'd.dolerite, metadolerite + amphibolite dykes, with plagioclase, hornblende, clinopyroxene, biotite, sphene + opaques; altered, occasion'ly foliated; ophitic texture||||||07-NOV-08
68745|Tournefort Metadolerite|64313|5|Briefly described|p450 Fig. 1, p468|Paleoproterozoic|Paleoproterozoic|Age: >1800Ma. Geological province: Gawler Craton. A suite of mafic dykes formerly referred to as the "Tournefort dykes". Intruded the Donington Suite at ca.1815Ma.||||||09-FEB-10
68745|Tournefort Metadolerite|65375|4|Described|p7, p13, p18, p45.|Paleoproterozoic|Paleoproterozoic|Yorke Peninsula. Formerly Tournefort Dyke Swarm of Parker et al. (1987). Five generations of dykes have been identified on basis of cross-cutting relationships.|1812 +/- 5 Ma.|||Intrudes Gleesons Landing and Royston Granites.|Undifferentiated dolerite, metadolerite or amphibolite dykes.|
68745|Tournefort Metadolerite|66302|5|Briefly described|p28, p63|Orosirian|Orosirian||1812 +/- 5 Ma (Schaefer, 1998)|||Intrudes the Donington Suite.||
68745|Tournefort Metadolerite|67323|6|Mentioned|Eastern Australia Time-Space Plot|||Southern Gawler Craton.||||||
68745|Tournefort Metadolerite|71129|6|Mentioned|p18|Orosirian|Orosirian|Geological Province: Spencer Domain, Gawler Craton.|1815 Ma|||||
68745|Tournefort Metadolerite|71317|5|Briefly described|p16|Palaeoproterozoic|Palaeoproterozoic|Spencer Domain, Gawler Craton.|c. 1815 Ma|||||
68745|Tournefort Metadolerite|71859|5|Briefly described|p4|Orosirian|Orosirian|Spencer Domain, southern Gawler Craton.|1815 Ma|||||
68745|Tournefort Metadolerite|72090|6|Mentioned|p10|Orosirian|Orosirian|Spencer Domain, Gawler Craton.|c. 1815 Ma|||||
68745|Tournefort Metadolerite|73107|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Gawler Craton: Yorke Peninsula, islands of Investigator Strait and DDH Investigator 1.|c. 1800 Ma|||Intrudes Royston Granite.|Undifferentiated dolerite, metadolerite and amphibolite dykes, with plagioclase, hornblende, clinopyroxene, biotite, sphene and opaques. Altered, occasionally foliated. Ophitic texture.|11-FEB-23
68745|Tournefort Metadolerite|73122|5|Briefly described|p17, 19, 21, 23-24, 26-41, 43|||The author has creatively referred to this unit in myriad nomenclatural variations; all mentions of Tournefort are gathered in this, the currently formal, version. Sourced from a long-lived, enriched lithospheric mantle tholeiitic melt. Petrology, mineralogy and deformation detailed.|1840-1810 Ma.|||Intrudes Donington Suite.|Voluminous Fe-rich tholeiitic dykes; planar, <10m wide.|
68745|Tournefort Metadolerite|73235|6|Mentioned|p53|Orosirian|Orosirian||c. 1810 Ma|||||
68745|Tournefort Metadolerite|73493|5|Briefly described|p713, p716 Fig.3, p732|||Gawler Craton, Eyre Peninsula. Previously correlated with Daly Head Metadolerite in regional mapping, this study suggests that correlation is incorrect and defines Daly Head Metadolerite as a new unit.|||||Mafic dyke or sill.|
68745|Tournefort Metadolerite|73525|5|Briefly described|p19 Fig.13|Orosirian|Orosirian|Spencer Domain, Olympic Domain.|1812+/-5 Ma crystallisation age||||Mafic intrusive.|
68745|Tournefort Metadolerite|73634|5|Briefly described|p3-6, 8, 11-13, 15, 17-18|||Eyre Peninsula, Gawler Craton. Spatially associated with occurrence of numerous shear zones (Kimban Orogeny 1730-1690 Ma). Usually referred to in the text as Tournefort Metadolerite Dykes or, less formally, as Tournefort dyke(s). Microstructure discussed in detail.|~1800 Ma.|||Intrudes Donington Suite, Wanna Megacrystic Granite Gneiss and Jussieu Metadolerite.|Dykes and sills. Sub-solidus amphibolite facies equivalent of MORB-derived melts.|
27591|Tregolana Shale Member|23805|5|Briefly described|p5 Fig. 3|Neoproterozoic|Neoproterozoic|Of the Tent Hill Formation (Wilpena Group).  Geological Province: Gawler Craton.||||||
27591|Tregolana Shale Member|23818|6|Mentioned|p74|||Of the Tent Hill Formation.||||||
27591|Tregolana Shale Member|24321|5|Briefly described|Map legend|Late Adelaidean|Late Adelaidean|Parent: Tent Hill Formation||||||
27591|Tregolana Shale Member|30801|6|Mentioned|p5|||Marinoan. Table P5-6||||||
27591|Tregolana Shale Member|30802|6|Mentioned|p12|||||||||
27591|Tregolana Shale Member|30807|6|Mentioned|p102|||Suggested map symbol||||||
27591|Tregolana Shale Member|31395|6|Mentioned|p64|||||||||
27591|Tregolana Shale Member|31540|6|Mentioned|p10|||Equiv. Woomera Shale Mb.||||||
27591|Tregolana Shale Member|32507|6|Mentioned|Table 3|||||||||
27591|Tregolana Shale Member|33474|6|Mentioned|Fig.3|||||||||
27591|Tregolana Shale Member|34319|5|Briefly described|p69|||||||||
27591|Tregolana Shale Member|34535|6|Mentioned|p74|||||||||
27591|Tregolana Shale Member|34536|6|Mentioned|Map legend|Adelaidean|Adelaidean|Marinoan||||||
27591|Tregolana Shale Member|34933|5|Briefly described|p60|||||||||
27591|Tregolana Shale Member|39807|6|Mentioned|p225|||||||||
27591|Tregolana Shale Member|39808|6|Mentioned|p223|||||||||
27591|Tregolana Shale Member|40448|5|Briefly described|p38|||||||||
27591|Tregolana Shale Member|42469|4|Described|p24|||||||||
27591|Tregolana Shale Member|42600|5|Briefly described|Table 1 P2|||||||||
27591|Tregolana Shale Member|42721|5|Briefly described|map legend|Marinoan||||||||
27591|Tregolana Shale Member|43052|5|Briefly described|p192,table 6.1|||of Tent Hill Formation||||||
27591|Tregolana Shale Member|43094|4|Described|Table 5|||of Tent Hill Formation||||||
27591|Tregolana Shale Member|44660|14|Not recorded|map legend|||Marinoan.||||||
27591|Tregolana Shale Member|60955|5|Briefly described|Map Legend|||Equivalent to Woomera Shale Member.||||||
27591|Tregolana Shale Member|67127|6|Mentioned|p104|Neoproterozoic|Neoproterozoic|South Australia.||Wilpena Group||Underlies the Arcoona Quartzite Member. Unconformably overlies the Roxby Downs Granite.||
27591|Tregolana Shale Member|70333|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Parent Formation not named.|||||Shale, red and green; siltstone.|
27591|Tregolana Shale Member|70334|4|Described|p56-58,66-67,77,88,92|Ediacaran|Ediacaran|Geological province: Gawler Craton. Of Stuart Shelf. Fine-laminated siltstones and shales deposited after marine transgression over the Stuart Shelf.||Unit of Tent Hill Formation.||Overlain by Corraberra Sandstone Member. Underlain by Whyalla Sandstone.|Chocolate shale and siltstone with green shale laminations and fine-grained red sandstone laminae, increasding in frequency and thickness up-section.|
27591|Tregolana Shale Member|70406|4|Described|p121-122, 120, 126,128, 117|Neoproterozoic|Neoproterozoic|~60m thick. Deposited below storm wave base. Misspelt as Tregolana Siltstone Member p119 Fig. 3.||Of Tent Hill Formation||Grades up into Lincoln Gap Siltstone Member. Lateral eqivalent of Moolooloo Siltstone member of Brachina Formation.|Laminated to thin-bedded, very fine to fine-grained, dark greyish brown sandstone interbedded with greyish red shale.|13-MAY-16
27591|Tregolana Shale Member|71037|5|Briefly described|p22-23 Fig.2|Neoproterozoic|Neoproterozoic|Shown only on the Six Mile Hill 1:75,000 surface geology map (p22-23 Fig.2).||Tent Hill Formation||Shown as younger than Whyalla Sandstone and underlies Lincoln Gap Siltstone Member.|Reddish brown laminated shale and siltstone, minor ripple crosslaminated sandstone; flute casts.|
27591|Tregolana Shale Member|71129|4|Described|p125-126,128-130,132,134,137-138|Ediacaran|Ediacaran|Of Stuart Shelf. Also referred to as Tregolana Member on p126. Thickness at type section: 60m (Dyson 1996). Also intersected 133.79m thick interval in MSDP02 drillhole. Occasionally exposed at the base of plateaus e.g. southern foothills of South Tent Hill but  largely obscured by colluvium flanking the plateaus. Occurs extensively in subsurface. Interpreted to be deposited at or below the storm wave base by waning, unidirectional currents (Dyson, 1996). Basal part of Tregolana Shale Member interpreted to be equivalent to Nuccaleena Formation. Intruded by Sugarloaf Dam Kimberlite sills. Equivalent to Nuccaleena Formation; correlable to Moolooloo Member/Brachina Fm. See also p141,145,152,164,174,209,225,227,229.||Unit of Tent Hill Formation.||Overlain unconformably by Sugarloaf Dam Sandstone. Conformably overlain by the Lincoln Gap Sandstone Member. Underlain unconformably by Whyalla Sandstone.|Laminated to thinly bedded greyish red to chocolate brown shales and siltstones with green shale laminations and reddish very fine- to fine-grained sandstone laminae and sandstones, which increase in frequency and thickness up sequence.|13-NOV-19
27591|Tregolana Shale Member|71130|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|||Tent Hill Formation.|||Reddish-brown laminated shale and siltstone, minor ripple cross-laminated sandstone; flute casts.|
27591|Tregolana Shale Member|71131|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|||Tent Hill Formation.|||Reddish-brown laminated shale and siltstone, minor ripple cross-laminated sandstone; flute casts.|
27591|Tregolana Shale Member|71895|5|Briefly described|p10,  p19, APP4. p4,  APP8. p201-p203|||Stuart Shelf. Spectral analysis is provided.||Wilpena Group||Overlies the Nuccaleena Formation.|Red-brown, olve-green to grey, very finely laminated marine, siltstone with minor, fine, sandstone horizons.|
27591|Tregolana Shale Member|72090|5|Briefly described|p37|||Gawler Craton.|||||Dark reddish brown to greyish brown, laminations, fine-grained, very well sorted interbedded shale and sandstone.|
27591|Tregolana Shale Member|72247|5|Briefly described|p41,43|Neoproterozoic|Neoproterozoic|Of Adelaide Geosyncline.||Unit of Wilpena Group.||Equivalent to Woomera Shale. Overlain by Corraberra Sandstone Member. Underlain by Nuccaleena Formation.||
27591|Tregolana Shale Member|73110|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic||||||Shale, red and green; siltstone.|
27591|Tregolana Shale Member|73226|6|Mentioned|p3|||||||||
27591|Tregolana Shale Member|73227|5|Briefly described|p25|Neoproterozoic|Neoproterozoic|Torrens Hinge Zone. May have acted as a caprock for mineralizing fluids in the underlying Whyalla Sandstone.||Tent Hill Formation, Wilpena Group||Underlain by Nuccaleena Formation. Overlain by Corraberra Sandstone Member. Equivalent to 'Woomera Shale'.|Reddish-brown laminated shale and siltstone.|
27591|Tregolana Shale Member|73234|6|Mentioned|p6-7, p9, p12-13, p20|||Deposited in low energy marine environments in greater water depths.||Tent Hill Formation, Wilpena Group||Unconformably overlain by Sugarloaf Dam Sandstone. Intruded by 'Sugarloaf Dam Kimberlite'||
27591|Tregolana Shale Member|74367|5|Briefly described|p8, p19|Ediacaran|Ediacaran|Previously Woomera Shale.|676+/-200 Ma Rb-Sr|Sandison Subgroup||Stratigraphically equivalent to Brachina Formation||
75892|Triangle Hill Granite|67540|3|Fully described|p25, p27 Tb.1,  p28 Tb.2|Calymmian|Calymmian|Type locality occurs at Triangle Hill, 35 km NNW of Olary. Curnamona Province: Olary Domain. S-type granite.Definition reference: this article and Fricke and Hore (2011).|~1590-1581 Ma|Of the Bimbowrie Suite.||Intrudes Ameroo Subsuite and the Tommie Wattie Formation.|Pink to buff or cream, medium- to coarse-grained, equigranular muscovite-biotite-quartz-plagioclase monzogranite; characterised by large K-feldspar phenocrysts. S-type.|08-FEB-16
75892|Triangle Hill Granite|69650|2|Defined|p4 Tb.1, p5 Tb.2, p12, p16-18|Calymmian|Calymmian|New name, after Triangle Hill, 35 km NW of Olary; also the type locality (described). Geochemistry, geochronology outlined.|c.1590-1581 Ma.|Unit in Bimbowrie Suite.||Intrudes Ameroo Subsuite and Tommie Wattie Formation.|Pink to buff or cream, medium- to coarse-grained, equigranular muscovite-biotite-quartz-plagioclase monzogranite; characterised by large K-feldspar phenocrysts. S-type.|08-FEB-16
75892|Triangle Hill Granite|70658|5|Briefly described|p33-34, 36|Mesoproterozoic|Mesoproterozoic|Olary Domain, Curnamona Province. Geochemistry briefly described. Forms large domal outcrops.|c.1590-1581 Ma.|Bimbowrie Suite.|||Pink to buff or cream, medium- to coarse-grained, equigranular muscovite-biotite-quartz-plagioclase monzogranite; characterised by large K-feldspar phenocrysts.|
25554|Trinity Well Sandstone Member|9862|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Of the Marree Formation. Basal cross-bedded sandstone and conglomerate.||||||
25554|Trinity Well Sandstone Member|23818|5|Briefly described|p152|Early Cretaceous|Early Cretaceous|Of the Marree Formation. Contains molluscs and foraminifera.||||||
25554|Trinity Well Sandstone Member|24175|5|Briefly described|p17 Fig. 3|Aptian|Barremian|Geological Province: Eromanga Basin.||||||
25554|Trinity Well Sandstone Member|30177|6|Mentioned|p102|||Member of Marree Formation.||||||
25554|Trinity Well Sandstone Member|33939|5|Briefly described|p413|||Neocomian to early Aptian.||||||
25554|Trinity Well Sandstone Member|34611|5|Briefly described|p153|||||||||
25554|Trinity Well Sandstone Member|38068|6|Mentioned|p71|||||||||
25554|Trinity Well Sandstone Member|40926|6|Mentioned|Table 2|||||||||
25554|Trinity Well Sandstone Member|44133|5|Briefly described|p112|Cretaceous|Cretaceous|Of the Cadna-owie Formation. Geological Province: Eromanga Basin.||||||
25554|Trinity Well Sandstone Member|65385|5|Briefly described|pS134 Fig.7|Early Cretaceous|Early Cretaceous|Of Cadna-owie Formation.||||||08-MAR-12
25554|Trinity Well Sandstone Member|68068|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Eromanga Basin. ||Unit in Parabarana Sandstone.||||
25554|Trinity Well Sandstone Member|68713|5|Briefly described|p22|Cretaceous|Cretaceous|Type section occurs ~ 400 m north of Western Spur.||Of the Cadna-owie Formation.||||
25554|Trinity Well Sandstone Member|69019|5|Briefly described|p87-89.|||Of Forbes et al. (1965) and Forbes (1966). Formerly part of Bulldog Shale. Type section ~400 m NW of Western Spur. Thickness c.50 m. Is discussed as if belonging to both Cadna-owie Formation and its equivalent, the Parabarana Sandstone. Caps the latter on eroding mesas. Beach facies.||Unit in Cadna-owie Formation.|||Clean, medium-grained cross-bedded sandstone, typically gravelly to pebbly; Lingula fossils locally abundant.|
25554|Trinity Well Sandstone Member|69023|5|Briefly described|p93-94|||This cross-bedded packet had been included within Parabarana Sandstone by Ludbrook (1966), but was later named as a Member of Marree Formation by Forbes (1966). Here, Sheard (2009) gives reasons for including it in Parabarana Sandstone instead of Bulldog Shale (Marree Formation). Caps eroding mesas.||Unit in Parabarana Sandstone.|||A clean, typically gravelly to pebbly, cross-bedded sandstone; abundant marine mollusc fossils (Lingula sp.); fossil wood, leaf and frond impressions and cycad trunks form strandline hash.|
25554|Trinity Well Sandstone Member|69457|5|Briefly described|p41:7|Early Cretaceous|Early Cretaceous|Forbes (1966). Fluviatile-tidal sediments.||Of Cadna-owie Formation.||Stratigraphic equivalent to Wyandra Sandstone Member (Qld), Mt Anna Sandstone Member (in SA).||23-JAN-19
25554|Trinity Well Sandstone Member|69946|5|Briefly described|p19, p57|Early Cretaceous|Early Cretaceous|Eromanga Basin.||Unit in Cadna-owie Formation.||||
25554|Trinity Well Sandstone Member|70384|5|Briefly described|Map legend.|Cretaceous|Cretaceous|||Of Cadna-owie Formation.|||Ferruginous, pebbly, carbonate-cemented sandstone; medium- to coarse-grained feldspathic sandstone, usually as distinctive cross-beds in the top 1-3m of the parent Formation.|23-JAN-19
25554|Trinity Well Sandstone Member|71342|5|Briefly described|Ch5 p57|Aptian|Barremian|Eromanga Basin. Spore-pollen zone is given in Ch5 p57.||Cadna-owie Formation||||
25554|Trinity Well Sandstone Member|72456|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Marree 1:250k map sheet. |||||Sandstone, pebbly, ferruginous, carbonate cemented; sandstone, medium to coarse-grained, feldspathic with crossbedding.|
26184|Truro Volcanics|14019|5|Briefly described|p20|Early Cambrian|Early Cambrian|Geological Province: Stansbury Basin. Correlative of the Antrim Plateau Volcanics.||||||
26184|Truro Volcanics|22581|6|Mentioned|Fig.2,p37|||Normanville Group, Kanmantoo Basin. Overlies Heatherdale Shale. Overlain by Carrickalinga Head Formation||||||
26184|Truro Volcanics|22643|5|Briefly described|p186, fig3,6|Early Cambrian|Early Cambrian|||||||
26184|Truro Volcanics|22671|6|Mentioned|p847-48|||Generally equated with the top of Normanville Group. Geological Province: Kanmantoo Belt (eastern South Australia).||||||18-JAN-06
26184|Truro Volcanics|22766|4|Described|Fig.2 p561, p562|Early Cambrian|Early Cambrian|See also Fig.1 p561.||||||26-FEB-07
26184|Truro Volcanics|22830|6|Mentioned|P25|||Interbedded with Heatherdale Shale||||||
26184|Truro Volcanics|22857|5|Briefly described|p88 Fig. 14.7A, p93-94|Early Cambrian|Early Cambrian|Of the Normanville Group. Max. thickness: 300m. ||||||
26184|Truro Volcanics|22858|5|Briefly described|p93|||||||||
26184|Truro Volcanics|23023|6|Mentioned|p1800|||||||||
26184|Truro Volcanics|23309|5|Briefly described|p25-27, Table 2.1, 2.3|Cambrian|Cambrian|of the Normanville Group||||||05-NOV-07
26184|Truro Volcanics|23818|4|Described|p98|Cambrian|Cambrian|Max. thickness: 2000 ft. Overlain by Hawker Group. Underlain by Umberatana Group (unconformable).||||||26-FEB-07
26184|Truro Volcanics|23854|5|Briefly described|p863|Early Cambrian|Early Cambrian|||||||
26184|Truro Volcanics|23869|5|Briefly described|p15 Fig. 3|Cambrian|Cambrian|||||||
26184|Truro Volcanics|23914|6|Mentioned|p158 Fig. 12|||||||||
26184|Truro Volcanics|23932|5|Briefly described|p665 Table 1|Early Cambrian|Early Cambrian|Geological Province: Adelaide Fold Belt.  Age: 525 Ma.||||||
26184|Truro Volcanics|23981|5|Briefly described|p8-9 Fig. 4, p22|Early Cambrian|Early Cambrian|Overlies Fork Tree Limestone. Interfingers with Heatherdale Shale. Geological Province: Stansbury Basin (Fleurieu Peninsula). See also p50.||||||
26184|Truro Volcanics|24465|5|Briefly described|p345 Fig.2|Early Cambrian|Early Cambrian|Of the Normanville Group.  Geological Province: Stansbury Basin.||||||19-JAN-05
26184|Truro Volcanics|24509|5|Briefly described|p42, p39 Fig. 1|Early Cambrian|Early Cambrian|Alkaline volcanics. Age: 525Ma. 300+m of altered vesicular and amygdaloidal andesite, trachyte and metabasalt. Geological Province: Adelaide Geosyncline.||||||04-MAY-05
26184|Truro Volcanics|24551|5|Briefly described|p74|||Of Normanville Group.||||||
26184|Truro Volcanics|30801|6|Mentioned|p5|||Lower Cambrian. Table P5-6||||||
26184|Truro Volcanics|30805|2|Defined|p1|Early Cambrian|Early Cambrian|See also p2-5.||||||26-FEB-07
26184|Truro Volcanics|30807|6|Mentioned|p102|||Suggested map symbol||||||
26184|Truro Volcanics|33471|5|Briefly described|p555|||||||||
26184|Truro Volcanics|34536|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
26184|Truro Volcanics|34612|6|Mentioned|p98|||Cambrian||||||
26184|Truro Volcanics|36534|6|Mentioned|p221|||||||||
26184|Truro Volcanics|39352|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
26184|Truro Volcanics|39489|4|Described|p8|||||||||
26184|Truro Volcanics|40442|6|Mentioned|p13|||||||||
26184|Truro Volcanics|40856|6|Mentioned|Fig.23.6|||||||||
26184|Truro Volcanics|41526|6|Mentioned|p61|||||||||
26184|Truro Volcanics|42222|5|Briefly described|p21|||||||||
26184|Truro Volcanics|42246|6|Mentioned|p17|||||||||
26184|Truro Volcanics|42266|6|Mentioned|Fig.2 P292|||||||||
26184|Truro Volcanics|42272|5|Briefly described|p404|||||||||
26184|Truro Volcanics|42274|6|Mentioned|p458|||||||||
26184|Truro Volcanics|42275|5|Briefly described|p468|||||||||
26184|Truro Volcanics|43053|5|Briefly described|Map Legend|Cambrian|Cambrian|Mafic to intermediate.||||||25-MAY-05
26184|Truro Volcanics|43195|5|Briefly described|Map Legend||Cambrian|See also commentary on back of map.||||||
26184|Truro Volcanics|43258|5|Briefly described|Map Legend||Cambrian|||||||
26184|Truro Volcanics|43298|5|Briefly described|Map Legend||Cambrian|||||||
26184|Truro Volcanics|43560|6|Mentioned|p235|||Maybe Truro tuff||||||
26184|Truro Volcanics|43781|6|Mentioned|p3||Botoman|SHRIMP Zircon age: 526+/-4 Ma||||||
26184|Truro Volcanics|44093|6|Mentioned|p108|||Intraplate basalt.||||||
26184|Truro Volcanics|44133|4|Described|p4 Fig. 7.2, 6, 13, 51 Fig. 7.18|Early Cambrian|Early Cambrian|Geological Province: Stansbury Basin. Of the Normanville Group. Maximum Thickness: 300m+.||||||
26184|Truro Volcanics|50154|2|Defined|p23, p52, p159|Early Cambrian|Early Cambrian|Of the Moralana Supergroup. Interlayered with the Nangeela Formation. Intruded by the Dergholm Granite. Geological Province: Glenelg Zone, Delamerian Fold Belt.||||||15-SEP-04
26184|Truro Volcanics|50156|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of Moralana Supergroup||||||
26184|Truro Volcanics|50157|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|||||||
26184|Truro Volcanics|50158|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of Moralana Supergroup||||||
26184|Truro Volcanics|50159|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|||||||22-JUN-04
26184|Truro Volcanics|50160|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of Moralana Supergroup||||||
26184|Truro Volcanics|50161|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of Moralana Supergroup.||||||
26184|Truro Volcanics|50162|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of Moralana Supergroup||||||
26184|Truro Volcanics|50163|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of Moralana Supergroup||||||
26184|Truro Volcanics|50164|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of Glenelg River Metamorphic Complex (Moralana Supergroup).||||||
26184|Truro Volcanics|60567|5|Briefly described|p39|Cambrian|Cambrian|Age: 526+/-4Ma (Cooper et al, 1992).||||||
26184|Truro Volcanics|60953|5|Briefly described|Map Legend|Cambrian|Cambrian|Mafic to intermediate volcanics.||||||
26184|Truro Volcanics|61046|5|Briefly described|p7 Fig. 1, p8 Fig. 2|||Of Normanville Group. Basic.||||||
26184|Truro Volcanics|61108|5|Briefly described|map legend|Cambrian|Cambrian|Mafic to intermediate volcanic rock.||||||
26184|Truro Volcanics|61307|5|Briefly described|p6 Fig. 3|Cambrian|Cambrian|Of the Normanville Group. Interfingers with Heatherdale Shale. Geological Province: Karinya Syncline/Adelaide Fold Belt. See also p14 Fig. 6||||||
26184|Truro Volcanics|62744|6|Mentioned|p708|||Of the Normanville Group. In western Victoria.||||||
26184|Truro Volcanics|63848|6|Mentioned|p532,  p534 Fig.4.|||||Unit in Normanville Group.||||
26184|Truro Volcanics|65337|5|Briefly described|p95.|Early Cambrian|Early Cambrian|Stansbury Basin. Correlative with Kalkarindji Volcanic Group.||Unit in Gnalta Group.||||
26184|Truro Volcanics|65489|6|Mentioned|p119|||Stansbury Basin.||||Correlates with Mooracoochie Volcanics (Warburton Basin).||
26184|Truro Volcanics|65716|4|Described|p3-9|Cryogenian|Cryogenian|From Chetwynd and part of Casterton 1:50k sheets. Sample dated is metagabbro. SHRIMP zircon U-Pb magmatic age of 642.5 +/- 3.9 Ma. Age conflicts with younger age of enclosing Moralana Supergroup sediments.||||||
26184|Truro Volcanics|65892|5|Briefly described|p9 Fig.4, p17. |Early Cambrian|Early Cambrian|Fleurieu Peninsula.||Unit in Normanville Group.||Overlies Fork Tree Limestone. Is unconformably overlain by Carrickalinga Head Formation.||
26184|Truro Volcanics|66002|5|Briefly described|p4 Tb.1|Cambrian|Cambrian|Of Moralana Supergroup. Defined by Forbes (1972). See also Morand et al. 2003.||||||
26184|Truro Volcanics|66623|6|Mentioned|p14, p427.|Middle Cambrian|Middle Cambrian|Strong geochemical correlation with Mount Arrowsmith Volcanics of Koonenberry Belt, although the authors point to problems involving location and age of the samples examined.||||||
26184|Truro Volcanics|67536|5|Briefly described|Map Legend|||Kanmantoo Province; basement to Murray Basin.||||Intercalated with Normanville and/or Kanmantoo Group metasediments.|Mafic to intermediate volcanic rocks.|
26184|Truro Volcanics|68116|5|Briefly described|Appendix, Map 29.|Early Cambrian|Early Cambrian|Contains  thin interbeds of slate and greywacke. Low regional metamorphic grade, commonly cleaved.|||||Mafic to felsic lavas and intrusives: basalt, andesite dark green, fine-grained; rhyolite cream, quartz-phyric; dolerite and gabbro: dark green; diorite dykes and sills: grey-green; mafic volcaniclastic sandstone and granulestone: dark grey-green.|
26184|Truro Volcanics|68735|6|Mentioned|p233 Fig.2, p235 Fig.3|Early Cambrian|Early Cambrian|Stansbury Basin.||Normanville Group.||||10-APR-17
26184|Truro Volcanics|68822|5|Briefly described|p324|Stage 2|Stage 2||ca. 522 Ma|Of the Normanville Group.|||Alkalic volcanics.|
26184|Truro Volcanics|68993|6|Mentioned|p544 Fig.1|Early Cambrian|Early Cambrian|Fleurieu Peninsula.||Of the Normanville Group.||||
26184|Truro Volcanics|69445|6|Mentioned|p30:17|Early Cambrian|Early Cambrian|Stansbury Basin.||||||12-JUL-16
26184|Truro Volcanics|69873|6|Mentioned|p85|Ediacaran|Ediacaran|Koonenberry Belt. An example of ~580 Ma rift tholeiites found along much of the 'Tasman Line' and through King Island to Tasmania.||||||
26184|Truro Volcanics|71139|6|Mentioned|p153-155, 157, 161|||Adelaide Geosyncline. Pb, Th, U concentrations and Pb isotope data tabulated.||||Interbedded with Kanmantoo Group sediments.|Alkali volcanics.|
26184|Truro Volcanics|71322|5|Briefly described|p51, p52 Fig.1, p53, p57, p60, p66, p73|Early Cambrian|Early Cambrian|Tentatively correlated with a volcano-sedimentary sequence in drillhole DEL 10ACD001 in the Haylands Cu-Au prospect near Morgan. This c.511 Ma age is of a tuffaceous siltstone from DEL 10ACD001. Other ages given with interpretations.|511 +/- 5 Ma (maximum depositional age).|Normanville Group.||Intercalated with Normanville and/or Kanmantoo Group. Provisionally correlated with Marne River Volcanics.|Mafic volcanics.|14-DEC-21
26184|Truro Volcanics|71593|4|Described|p8, p12, p19-p22, p102||Early Cambrian|Glenelg Zone. Early Cambrian age for this unit derived from SHRIMP U/Pb dates of correlatives which yielded ages of 521 +/- 4 Ma and 522 +/- 2 Ma (Cooper et al, 1992; Burtt et al, 2000; Jenkins et al, 2002). See also p121-p122, p133, p166, p169-p172, p177, p180, p195, p198, p202.|c. 525 Ma|||Overlain by the Kanmantoo Group.|Basaltic dykes, mafic to felsic igneous rocks and associated volcanics.|
26184|Truro Volcanics|72445|6|Mentioned|App.7 p6 Fig.3.|Cambrian|Cambrian|Shown only on the geological map covering the Stavely Project area (from Geology of Victoria 2003: 21).||||||
26184|Truro Volcanics|73118|6|Mentioned|p73|||Probably related to early Delamerian Orogeny.|526 Ma; Cooper et al., 1992).|||||
26184|Truro Volcanics|73188|6|Mentioned|p353|||Evidence of extensional tectonism.|||||Mafic intraplate lavas.|
26184|Truro Volcanics|73430|5|Briefly described|p492, p497-498, p508 Fig.8|Early Cambrian|Early Cambrian|Mostly outcrops on the flanks of the Karinya syncline to the north and northeast of Adelaide. MgO-rich and high compatible elements suggest the alkali basalts are near-primary unfractionated melts. High eNd values of +5 to +7.8. Equated with a deformed alkaline mafic suite hosted in the Harvester's Creek greywacke by Gibson et al., (2015). See also Turo alkali basalt lavas p493, Truro volcanics p493, p508, p517, Truro basalts p503 Fig.6, Truro suite p498, p516.|522+/-2 Ma|Normanville Group|||Suite of undersaturated anorogenic style alkali basalts. Highly alkaline basaltic lava flows, variably deformed, metamorphosed and altered.|
26284|Tuit Member|22528|6|Mentioned|p43 Fig2||Late Eocene|||||||
26284|Tuit Member|22541|5|Briefly described|p 24, Fig 1, 7|||||||||
26284|Tuit Member|38621|2|Defined|p6|late Eocene|late Eocene|||||||
26284|Tuit Member|40238|5|Briefly described|p125|||||||||
26284|Tuit Member|40429|6|Mentioned|Fig.2|||||||||
26284|Tuit Member|40453|6|Mentioned|Fig.5|||||||||
26284|Tuit Member|40778|6|Mentioned|p529|||||||||
26284|Tuit Member|40877|5|Briefly described|p49|||||||||
26284|Tuit Member|40969|6|Mentioned|Fig.1|||||||||
26284|Tuit Member|41025|6|Mentioned|Fig.3|||||||||
26284|Tuit Member|41513|6|Mentioned|p44|||||||||
26284|Tuit Member|41520|6|Mentioned|Fig.10|||||||||
26284|Tuit Member|42498|6|Mentioned|Map Legend|Eocene|Eocene|||||||
26284|Tuit Member|42506|5|Briefly described|Map legend|Eocene||Age Tertiary||||||
26284|Tuit Member|44133|5|Briefly described|p165 Fig. 10.11, 168|Late Eocene|Late Eocene|Geological Province: Saint Vincent Basin. Of the Blanche Point Formation.||||||
26284|Tuit Member|60538|5|Briefly described|p479 Fig. 18|Oligocene|Eocene|Geological Province: Saint Vincent Basin. Of the Blanche Point Formation. Shown as overlying or at least younger than the Perkana Member.||||||18-MAR-13
26284|Tuit Member|64397|5|Briefly described|p233 Fig. 2|Late Eocene|Late Eocene|Hard (silica-rich) and soft (carbonate-rich) layers. Geological province: St Vincent Basin.||||||
26284|Tuit Member|64993|5|Briefly described|p26|||Of the Blanche Point Formation. Geological province: St Vincent Basin. Contains a molluscan assemblage (Cypraeidae), preserved as moulds.||||||26-MAR-09
26284|Tuit Member|65891|5|Briefly described|p221 Fig.5, p222 Fig.7, p228 Fig.11.|Paleogene|Paleogene|Topmost unit in Blanche Point Formation, above Perkana Member. Priabonian age. Spirocolpus-rich.||||||
26284|Tuit Member|70660|5|Briefly described|p9, p12, p17 fig 9a, 9b|Late Priabonian|Late Priabonian|See also p18, p25-p26, p28, p33, p46.||Blanche Point Formation||Overlies the Perkana Member. Overlain by the Chinaman Gully Formation.||
26284|Tuit Member|70722|5|Briefly described|p218|Late Eocene|Late Eocene|Of St. Vincent Basin. Equivalent to Kingscote Limestone Unit K1 of this study.||Unit of Blanche Point Formation.||Uppermost unit of Blanche Point Formation. Overlain by Chinaman Gully Formation. Underlain by Perkana Member.||
26284|Tuit Member|73188|6|Mentioned|p320|Late Eocene|Late Eocene|St Vincent Basin.||Blanche Point Formation||||
25681|Tuketja Member|22528|6|Mentioned|p43 Fig2||Late Eocene|||||||
25681|Tuketja Member|22541|4|Described|p 22, Fig 1, 7|||Blanche Point Formation||||||
25681|Tuketja Member|23010|6|Mentioned|p339|||||||||
25681|Tuketja Member|38621|2|Defined|p3|late Eocene|late Eocene|||||||
25681|Tuketja Member|40238|5|Briefly described|p125|||||||||
25681|Tuketja Member|40429|6|Mentioned|Fig.2|||||||||
25681|Tuketja Member|40453|6|Mentioned|Fig.5|||||||||
25681|Tuketja Member|40778|6|Mentioned|p530|||||||||
25681|Tuketja Member|40877|5|Briefly described|p47|||||||||
25681|Tuketja Member|40969|5|Briefly described|p7|||||||||
25681|Tuketja Member|41025|6|Mentioned|Fig.3|||||||||
25681|Tuketja Member|41513|6|Mentioned|p43|||||||||
25681|Tuketja Member|41520|6|Mentioned|p191|||||||||
25681|Tuketja Member|41626|6|Mentioned|p54|||||||||
25681|Tuketja Member|42443|6|Mentioned|p7|||||||||
25681|Tuketja Member|42461|5|Briefly described|p87|late Eocene||of Blanche Point Formation||||||
25681|Tuketja Member|42574|6|Mentioned|Fig.2 P242|||||||||
25681|Tuketja Member|44133|5|Briefly described|p165 Fig. 10.11, 168|Late Eocene|Late Eocene|Geological Province: Saint Vincent Basin. Of the Blanche Point Formation. Underlies: Gull Rock Member. ||||||
25681|Tuketja Member|60538|5|Briefly described|p479 Fig. 18|Oligocene|Eocene|Geological Province: Saint Vincent Basin. Of the Balance Point Formation.||||||
25681|Tuketja Member|64397|5|Briefly described|p233 Fig. 2|Late Eocene|Late Eocene|Calcareous, glauconitic marl. Geological province: St Vincent Basin.||||||
25681|Tuketja Member|65891|5|Briefly described|p221-222 Figs.5,7; p226; p228 Fig.11.|Paleogene|Paleogene|Basal unit in Blanche Point Formation. Richly glauconitic. Is overlain by Gull Rock Member.||||||
25681|Tuketja Member|70660|5|Briefly described|p9, p12, p15-p19, p25-p26, p28, p33|Early Priabonian|Early Priabonian|Fossils include bryozoans, nautiloids and molluscs.||Blanche Point Formation||Overlies the Tortachilla Limestone. Overlain by the Gull Rock Member.|Thin glauconitic and calcareous mudstone and clay with bands of fossiliferous limestone.|
25681|Tuketja Member|70722|5|Briefly described|p218|Late Eocene|Late Eocene|Of St. Vincent Basin. Equivalent to Kingscote Limestone Unit K1 of this study.||Unit of Blanche Point Formation.||Lowermost unit of Blanche Point Formation. Overlain by Gull Rock Member. Underlain by Tortachilla Limestone.||
25681|Tuketja Member|73188|6|Mentioned|p320|Late Eocene|Late Eocene|St Vincent Basin.||Blanche Point Formation||||
39567|Tungkillo Member|24465|4|Described|p353|Early Cambrian|Early Cambrian|Thin carbonate unit within the Backstairs Passage Formation?|||||Several marble - calc-silicate bands; banded grey to white marble varying to  banded green and white or greenish grey calc-silicate.|06-NOV-15
35382|Tunkillia Suite|24365|5|Briefly described|p4, p5 Fig.2|Statherian|Statherian|Includes deformed granodiorite gneiss. Age: 1690-1680 Ma. Geological Province: Gawler Craton.||||||26-NOV-04
35382|Tunkillia Suite|24422|5|Briefly described|p84 Fig. 1, p87|Paleoproterozoic|Paleoproterozoic|Age: ca. 1690-1620 Ma. Geological Province: Gawler Craton.||||||07-NOV-08
35382|Tunkillia Suite|24505|5|Briefly described|p5 Fig. 1, p8|||Geological Province: Gawler Craton.||||||
35382|Tunkillia Suite|24583|6|Mentioned|p12|||Geological Province: Gawler Craton.||||||06-MAY-05
35382|Tunkillia Suite|24597|5|Briefly described|p526 Fig. 1|Paleoproterozoic|Paleoproterozoic|Age: ca1680Ma. Geological Province: Gawler Craton.  See also p528 Fig. 3, p526.||||||07-NOV-08
35382|Tunkillia Suite|60484|2|Defined|p32, p33 Fig. 1|Statherian|Statherian|A suite of granitoids on CHILDARA, composed of four main units including the Tunkillia augen gneiss (TAG).  Age: ~1690-1670Ma.  Type section included.  Geological Province: Gawler Craton.||||||
35382|Tunkillia Suite|60515|6|Mentioned|p116 Fig.1 |||||||||
35382|Tunkillia Suite|60704|5|Briefly described|p685, p686 Fig.1|Paleoproterozoic|Paleoproterozoic|Age: ca. 1680 Ma (U-Pb zircon, Ferris and Schwarz, 2003).||||||23-DEC-08
35382|Tunkillia Suite|60716|5|Briefly described|p7|||Contains medium- to coarse-grained granitoids.||||||
35382|Tunkillia Suite|61393|5|Briefly described|p166 Fig.1, p167, p175, p177.|Paleoproterozoic|Paleoproterozoic|I-type, mafic to felsic magmatism.|c.1690-1680 Ma.|||||
35382|Tunkillia Suite|61522|5|Briefly described|p5 Fig.1|||Geological Province: Gawler Craton.||||||
35382|Tunkillia Suite|61659|5|Briefly described|p31 Fig.2, p33.  |Paleoproterozoic|Paleoproterozoic|Associated with magmatic arc processes.|1690-1680 Ma (Ferris et al. 2002).|||Intrudes Wilgena Domain.||
35382|Tunkillia Suite|61864|6|Mentioned|p16 fig 3|||||||||
35382|Tunkillia Suite|62641|5|Briefly described|p277 Fig.1, p278. |||Nuyts Domain. Subduction-related magmatic arc setting.|1690-1670 Ma||||Felsic intrusives.|
35382|Tunkillia Suite|62978|5|Briefly described|p161, p180|Mesoproterozoic||Intrusive rocks. Age: ~1680Ma. Geological Province: Gawler Craton.||||||07-FEB-11
35382|Tunkillia Suite|63020|5|Briefly described|p987 Fig. 8|Paleoproterozoic|Paleoproterozoic|Age: ~1680Ma. Geological Province: Gawler Craton (Nuyts Domain).||||||07-NOV-08
35382|Tunkillia Suite|63866|6|Mentioned|p9, p18, p31|Statherian|Statherian|Nuyts Domain, Gawler Craton.|c. 1680 Ma (U-Pb zircon)|||||
35382|Tunkillia Suite|64130|5|Briefly described|p1378,1380,1388 Figs.1,2,6; p1382   |Mesoproterozoic|Mesoproterozoic|I-type intrusives.|1690-1670 Ma|||||
35382|Tunkillia Suite|64137|5|Briefly described|p1542 Fig.1, p1543,   |Paleoproterozoic|Paleoproterozoic|Dominant host of gold at Tunkillia (Nuyts domain); also at Nuckulla Hill and Barns.|~1680 Ma (U-Pb zircon; Ferris, 2001).|||||
35382|Tunkillia Suite|64576|6|Mentioned|p624, p625 Fig. 2|Paleoproterozoic|Paleoproterozoic|Age: 1690-1670Ma. ||||||
35382|Tunkillia Suite|64722|5|Briefly described|Fig. 2 p3-6, p14|Statherian|Statherian|A product of extensive granite magmatism in the Gawler Province that occurred mainly between 1690-1670 Ma.||||||12-APR-12
35382|Tunkillia Suite|64726|6|Mentioned|p82, p83 Fig.2, p88.|Paleoproterozoic|Paleoproterozoic|Western Gawler Craton. Episodic arc-type magmatism. Interpreted as relics of a continental arc emplaced in response to north-dipping subduction.|c.1740-1670 Ma.|||||
35382|Tunkillia Suite|64739|6|Mentioned|pp264-266, pp274-275, p278, p280.|Paleoproterozoic|Paleoproterozoic|Gawler Craton. Felsic to mafic plutons.|1690-1670 Ma.|||||
35382|Tunkillia Suite|64740|6|Mentioned|p284 Fig.1. |Paleoproterozoic|Paleoproterozoic|||||||
35382|Tunkillia Suite|64741|5|Briefly described|p299 Fig. 2|||||||||07-FEB-11
35382|Tunkillia Suite|64828|5|Briefly described|p1064 Fig. 1|Paleoproterozoic|Paleoproterozoic|Geological province: Gawler Craton.||||||04-MAR-09
35382|Tunkillia Suite|65376|5|Briefly described|p10, pp125-132, p172.|Mesoproterozoic|Paleoproterozoic|A recently-defined (2004) term for the I-type felsic and co-magmatic intermediate to mafic intrusives within the Gawler Craton that crystallised between 1690 and 1670 Ma.|1690-1670 Ma.||||The type-section granite is a foliated, medium-grained to megacrystic augen gneiss, with coarse K-feldspar, sericitised plagioclase, ribbon quartz and minor biotite.|
35382|Tunkillia Suite|65390|5|Briefly described|p21, p24|Statherian|Statherian|Of Ferris (2001). Comagmatic felsic and mafic granitoids within the Yarlbrinda Shear Zone. U-Pb zircon age of c. 1680 Ma. Arc-like geochemical signature. Ifould Suite is considered an equivalent.||||||
35382|Tunkillia Suite|65485|6|Mentioned|Fig 1|Paleoproterozoic|Paleoproterozoic|||||||19-MAR-12
35382|Tunkillia Suite|65487|6|Mentioned|p61|||Emplaced 1690-1670 Ma in the western Gawler Craton. Interpreted 'arc-like' geochemical signature.||||||
35382|Tunkillia Suite|65772|5|Briefly described|p227-239|Statherian|Statherian|Intrudes Christie Gneiss. Includes syenite, monzogranite, granodiorite and syenogranite. Isolated outcrops. 1690-1670 Ma. Late- to post-tectonic (Kimban Orogeny). Subduction-related arc setting not readily reconcilable with geochemistry/mineralogy.||||||
35382|Tunkillia Suite|65922|6|Mentioned|p13 Fig. 4|||Gawler Craton.||||||
35382|Tunkillia Suite|66302|5|Briefly described|p4-5 Figs.3,4; p19, p21-p24, p34,p54-p56|Statherian|Statherian|Fowler and Nuyts Domains, Gawler Craton. Also given are U-Pb zircon ages of 1686 +/- 5 Ma, 1680 +/-9 Ma and 1669 +/- 13 Ma (Fanning et al, 2007). May have formed in a late to post tectonic setting representing the continuation of the Kimban Orogeny. See also p65, p67, p76 Fig.20.|1672 +/- 17 Ma (Teasdale 1997)||Includes the Symons Granite and the Paxton Granite.||Deformed, medium grained, equigranular leucocratic granite and adamellite.|
35382|Tunkillia Suite|66519|6|Mentioned|p32.|Paleoproterozoic|Paleoproterozoic|Gawler Craton.||||||
35382|Tunkillia Suite|67058|5|Briefly described|p497.|||Western Gawler Craton. Felsic magmatics. A possible source for the Tarcoola Formation.|1690-1670 Ma.|||||
35382|Tunkillia Suite|67117|6|Mentioned|Map legend.|||Shown in Solid Geology Interpretation 1:1M figure as '?Engenina Adamellite, Symons Granite, equivalents of Tunkilla Suite'.||||||03-MAY-13
35382|Tunkillia Suite|67323|5|Briefly described|Eastern Australia Time-Space Plot; p34|Paleoproterozoic|Paleoproterozoic|Western and central Gawler Craton. Emplaced in a continental back-arc setting.|~1670 Ma.||||Felsic granitoids.|
35382|Tunkillia Suite|67536|5|Briefly described|Map Legend|Statherian|Statherian|Gawler Craton.|1680 +/- 5 Ma - 1679 +/- 12 Ma||||Comagmatic felsic and mafic granitoid rocks.|
35382|Tunkillia Suite|67581|6|Mentioned|p44 Fig.8, p45||||1690-1670 Ma.|||||
35382|Tunkillia Suite|67980|6|Mentioned|p550, p564|Statherian|Statherian|Ferris and Schwarz (2004); Payne et al. (2010). Gawler Craton. Associated with Kimban Orogeny (c.1730-1690 Ma).||||||
35382|Tunkillia Suite|68131|5|Briefly described|p2 Fig.1, p93-96|Mesoproterozoic|Paleoproterozoic|Central Gawler Craton. Associated with the Kararan Orogeny. Hosts the Tunkillia gold deposit. Cut by a dacite dyke dated at 1586 +/- 9 Ma, setting a maximum constraint on the age of mineralisation.|c.1690-1670 Ma.||||Mafic to felsic intrusive rocks.|
35382|Tunkillia Suite|69004|6|Mentioned|p18|||Gawler Craton.||||||
35382|Tunkillia Suite|69048|6|Mentioned|p3|||Central-western Eyre Peninsula.||||||
35382|Tunkillia Suite|69554|6|Mentioned|p128|||Gawler Craton.|1690-1670 Ma.|||||
35382|Tunkillia Suite|69591|6|Mentioned|p107 Fig.2.103|||Appears in a diagram of the geodynamic setting of ~1690-1670 Ma eastern Australia. Backarc environment.||||||
35382|Tunkillia Suite|69648|5|Briefly described|p15-16|||Younger deformed granitoids on the western Gawler Craton (Daly et al, 1998).||||Ifould Complex considered as correlatives of part of the Tunkillia Suite (Ferris and Schwarz, 2004).||
35382|Tunkillia Suite|69649|5|Briefly described|p9-14, p6 Fig.4, p7, p8 Fig.6, p27|||See also p36-41, p52-56. Defined from outcrops as well as Helix Resources NL drillhole LED 10 in Area 223 of the Tunkillia gold prospect. Gold is hosted in quartz-sulfide veins. Ferris (2005) included the Ifould Complex of Teasdale (1997) in this Suite. Contains enclaves of andalusite-biotite hornfels basement. SHRIMP U-Pb zircon age of 1686 +/- 5 Ma (Fanning et al., 2006).|1690-1670 Ma.||||Co-magmatic I-type intrusives: orthogneiss, granite, mylonite; and rhyolite, mafic and aplite dykes.|23-FEB-15
35382|Tunkillia Suite|70027|6|Mentioned|p56,58|Statherian|Statherian|Geological province: Gawler Craton. Emplaced into Gawler Craton ca. 1690-1670 Ma post-Kimban Orogeny.|ca. 1690-1670 Ma|||||
35382|Tunkillia Suite|70337|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic||||||Orthogneiss, granitic to quartz syenitic; biotite granite, adamellite and granodiorite; minor mylonite; minor amphibolite, rhyolite, rhyodacite and aplite dykes.|
35382|Tunkillia Suite|70511|6|Mentioned|p87|Paleoproterozoic|Paleoproterozoic|Gawler Craton.|1690-1670 Ma.|||||
35382|Tunkillia Suite|70893|5|Briefly described|p1, p3 fig 1|Statherian|Statherian|Associated with the Kimban Orogeny. |1730-1690 Ma|||||
35382|Tunkillia Suite|70947|6|Mentioned|p960|Statherian|Statherian|Geological province: Gawler Craton.|1690-1670 Ma|||||
35382|Tunkillia Suite|71037|5|Briefly described|p21 Fig.1|Paleoproterozoic|Paleoproterozoic|Shown only on 'Outcropping geology and mineral deposits of northern Eyre Peninsula' map p21 Fig.1.||||Shown as younger than Pinbong Suite and older than Corunna Conglomerate.||
35382|Tunkillia Suite|71043|6|Mentioned|p104, p107|Statherian|Statherian|Payne et al. (2010). Gawler Craton.|1690-1670 Ma.|||||
35382|Tunkillia Suite|71317|4|Described|p1, p14-p16, p19, p114|Late Palaeoproterozoic||Nuyts Domain, Gawler Craton. Mistakenly referred to as the Tunkillia Supersuite on p19 and p20 in reference to Ferris and Faulkner 2007. Together with the Peter Pan Supersuite and St Peter Suite forms the basement on the Peltabinna mapsheet.|1690-1670 Ma|||Overlain by the Gawler Range Volcanics.|Granite to diorite plutons and rhyolite and mafic dykes.|05-SEP-19
35382|Tunkillia Suite|71318|5|Briefly described|p3,9,34,50|Paleoproterozoic|Paleoproterozoic|Geological province: Gawler Craton. Sample GSSA 2017953 (qtz-plg-k-spar-bt granite) yielded an interpreted (weighted mean 207Pb/206Pb age) magmatic crystallisation age of 1688+\-16 Ma. Sample GSSA 2017967 (medium-grained inequigranular granite) yielded an interpreted (weighted mean 207Pb/206Pb age) magmatic crystallisation age of 1732+\-15 Ma, with an inherited zircon population at 1791+\-19 Ma. Sample GSSA 2017972 (sericite-altered foliated granite) yielded an interpreted (weighted mean 207Pb/206Pb age) best estimate of magmatic crystallisation age of 1692+\-15 Ma. Zircon characteristics, petrography, U-Pb isotopic results by ICPMS and geochronological interpretation are provided.|||||Medium-grained, inequigranular granite dominated by quartz and feldspar.|28-OCT-22
35382|Tunkillia Suite|71341|6|Mentioned|p179 fig 1|Palaeoproterozoic|Palaeoproterozoic||ca. 1690-1670 Ma|||||
35382|Tunkillia Suite|71348|6|Mentioned|p201|Statherian|Statherian|Geological province: Gawler Craton.||||||
35382|Tunkillia Suite|71534|6|Mentioned|p295-296,301|Statherian|Statherian|Geological province: Gawler Craton. Late syn- to post-Kimban magmatism with a juvenile component (Payne et al., 2010).|c. 1690-1670 Ma|||||
35382|Tunkillia Suite|71559|6|Mentioned|p15 Fig 1, p16 Fig 2|Statherian|Statherian|Geological province: Gawler Craton.|1690-1670 Ma|||Basement includes Peter Pan Supersuite and Tunkillia Suite||
35382|Tunkillia Suite|71712|6|Mentioned|p411, 419|Statherian|Statherian|Eastern Gawler Craton. Located west of the Cariewerloo Basin.|~1690-1670 Ma|||||
35382|Tunkillia Suite|71859|5|Briefly described|p3, p6|Paleoproterozoic|Paleoproterozoic||c. 1690-1670 Ma||||Granite intrusions.|06-APR-23
35382|Tunkillia Suite|71862|5|Briefly described|p3-p6, p21|||Post-orogenic suite intruded after the Peter Pan Supersuite.|c. 1690-1670 Ma|||||
35382|Tunkillia Suite|72090|6|Mentioned|p9-p10, p14|Statherian|Statherian|Gawler Craton.|c. 1690-1670 Ma|||Overlain by the Gawler Range Volcanics.||
35382|Tunkillia Suite|72242|6|Mentioned|p27|Statherian|Statherian|Geological province: Coompana Province, Western Gawler Craton. Bimodal magmatism associated with Kimban Orogeny.||||||
35382|Tunkillia Suite|72462|6|Mentioned|p3|Paleoproterozoic|Paleoproterozoic|Gawler Craton.||||||
35382|Tunkillia Suite|72949|6|Mentioned|p34, p37-38|Statherian|Statherian|Transitional eNd values. eNd(1680 Ma) = -6.3 to 2.6 (Payne et al., 2010). Tectonic setting said to be conjectural.||||||
35382|Tunkillia Suite|73026|5|Briefly described|p6, p10,|Paleoproterozoic|Paleoproterozoic|Central/western Eyre Peninsula. Emplaced during the waning stages of the Kimban Orogeny.|c. 1690-1675 Ma|||||
35382|Tunkillia Suite|73027|5|Briefly described|p6, p9|Mesoproterozoic|Palaeoproterozoic|Central/western Eyre Peninsula. Emplaced during the waning phases of the Kimban Orogeny and represents a late to post orogenic magmatic event.|c. 1690 Ma-1670 Ma|||||
35382|Tunkillia Suite|73030|6|Mentioned|p2148-2150|Statherian|Statherian|Gawler Craton.|1690 - 1670 Ma|||||
35382|Tunkillia Suite|73104|5|Briefly described|p1-2, p5, p11, p25, p29, p32|Statherian|Statherian|Age range covers the magmatic crystallisation age of Nummee Granodiorite. Formed in a late-tectonic to post-tectonic setting, following the 1740-1690 Ma Kimban Orogeny. Occurs in the Fowler Domain in the western Gawler Craton and in an arcuate belt along the margins of the Nuyts Domain within the Yarlbrinda, Yerda and Oolabinnia shear zones.|c. 1690-1670 Ma||Nummee Granodiorite||Granitoids.|
35382|Tunkillia Suite|73112|5|Briefly described|Map legend.|||Shown in the Solid Geology Interpretation map, below the main Nullarbor 250k map. The Engenina Adamellite, Symons Granite, equivalents of Tunkillia Suite are all mapped as one unit.||||||
35382|Tunkillia Suite|73130|6|Mentioned|[poster] Fig.1|Paleoproterozoic|Paleoproterozoic|||||||28-OCT-22
35382|Tunkillia Suite|73155|6|Mentioned|p264 Fig.1|Statherian|Statherian|Gawler Craton.|1690-1670 Ma|||||
35382|Tunkillia Suite|73162|6|Mentioned|p449, Fig.1|Statherian|Statherian||1690-1670 Ma|||||
35382|Tunkillia Suite|73233|5|Briefly described|p27 Fig.1, p28, p30|Statherian|Statherian|Gawler Craton, Fowler Domain. Western Fowler Domain includes reworked Tunkillia Suite, deformed and metamorphosed during the Kimban Orogeny.|1730-1670 Ma||||Magmatic rocks including granite and deformed granite.|
35382|Tunkillia Suite|73234|6|Mentioned|p19|Statherian|Statherian|Eyre Peninsula, north-western.|c. 1690-1670 Ma||||Granitoids.|
35382|Tunkillia Suite|73235|6|Mentioned|p52-53, p63|Statherian|Statherian|Gawler Craton. Nuyts region. Hosts Tunkillia and Barns intrusion-related gold mineralisation. May be associated with intrusion-related mineralisation, although further research is required.  Hosts gold mineralisation in the Wudinna mineral field of the Kararan (Hiltaba Suite) gold mineral system.|1690-1670 Ma||||Includes felsic rocks.|
35382|Tunkillia Suite|73298|5|Briefly described|p1071, p1073, p1076-1077, p1079-1087|Statherian|Statherian|Gawler Craton, western. Periphery of the Nuyts Terrane. Outcrop is poor. More detailed descriptions are made by Chalmers (2009), Fanning et al. (2007), Ferris (2001), Payne et al. (2010), Reid et al. (2016), Swain et al. (2008), Teasdale (1997). I-type, interpreted as continental arc-derived or having a supra-subduction-related setting based on geochemical and isotopic characteristics, similar to St Peters Suite. Two sub-suites are distinguished from alkali feldspar Pb-isotopic signatures. The eastern Tunkillia Suite has Pb-isotope ratios indicative of crust-mantle mixing, the western Tunkillia Suite contains unradiogenic Pb-isotopic ratios inferred to be from a U-depleted and garnet bearing granulitic crustal component. Locations in text include p1072 Fig.1, p1074 Fig.2, p1078 Fig.6.|ca 1690-1670 Ma||||Diorites, granodiorites and granites. Includes medium- to coarse-grained, seriate- to porphyritic plutonic granitoids classified mostly as quartz monzogranite with weak to strong metamorphic fabric. Weak to absent alteration.|
35382|Tunkillia Suite|73302|5|Briefly described|p32-34, 53|||Cental Gawler Craton. Emplaced during the late Kimban (1730-1690 Ma) Orogeny. Comprises moderately juvenile crust that could have interacted with St Peter Suite magmas.|c.1690-1670 Ma.||||A series of moderately juvenile magmatic rocks.|
35382|Tunkillia Suite|73493|5|Briefly described|p712, p714 Fig.1, p716 Fig.3|Statherian|Statherian|Gawler Craton.|ca 1690-1670 Ma||||Granitic, and mafic.|
75788|Twenty Mile Hill Member|66884|2|Defined|p37-39, p41-44, incl Figs.2-4|||New name. Corresponds to strata measured by Belperio (1987; his sections 1 and 2). Type section: outcrops present between Mount Norwest Gorge and Old Mount North West Homestead (29o55.936'S, 138o1.363'E to 29o55.461'S, 138o1.847'E). Thickness: ~1350 m thick in type section, but thins to ~740 m adjacent to Witchelina diapir. Age: Mid Torrensian.||Skillogalee Dolomite||Conformably overlies Camel Flat Shale Member; is overlain by Old Mount North West Member; is disconformably overlain by Umberatana Group 2 km west of Trial Hole.|Brown weathered, dark blue-grey fresh, fine-grained, laminated, stromatolitic sandy dolostone interbedded with subordinate feldspathic quartz arenite.|14-DEC-16
28298|Uley Formation|23719|5|Briefly described|p29|||||||||
28298|Uley Formation|29664|2|Defined|p2|late Tertiary|late Tertiary|||||||
28298|Uley Formation|39349|6|Mentioned|Map legend|Pleistocene|Pliocene|Pliocene to Pleistocene||||||
28298|Uley Formation|40448|6|Mentioned|p43|||||||||
28298|Uley Formation|42716|6|Mentioned|Map legend|Pliocene||||||||
28298|Uley Formation|43049|6|Mentioned|p23|||||||||
28298|Uley Formation|44133|5|Briefly described|p153 Fig. 10.2|Late Pliocene|Early Pliocene|Geological Province: Eucla Basin. ||||||
28298|Uley Formation|61070|5|Briefly described|Map Legend|Late Pliocene|Early Pliocene|Well-sorted, rounded, orange-brown clayey sand and quartz sand unconformably overlying the Wanilla Formation.||||||12-JAN-10
28298|Uley Formation|61155|5|Briefly described|p17|Late Pliocene|Early Pliocene|Age: 4-2.5Ma. Thickness: 40m. Geological Province: Polda Basin, Eyre Peninsula.||||||
28298|Uley Formation|68811|6|Mentioned|p113 fig 66, p193 tbl 47|Tertiary|Tertiary|||||Overlies the Wanilla Formation. Overlain by Bridgewater Formation.||16-APR-20
27596|Ulupa Siltstone|22631|6|Mentioned|p178|||||||||
27596|Ulupa Siltstone|22772|5|Briefly described|Table13.1|Neoproterozoic III|Neoproterozoic III|||||||
27596|Ulupa Siltstone|22857|5|Briefly described|Tb. 13.1 (insert p70-71)|Marinoan|Marinoan|Of the Wilpena Group.||||||
27596|Ulupa Siltstone|23287|6|Mentioned|Fig.2|||Age: Lower Ediacarian. of Stuart Shelf.||||||
27596|Ulupa Siltstone|23288|6|Mentioned|Fig.5|||||||||
27596|Ulupa Siltstone|23394|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of Wilpena Group||||||
27596|Ulupa Siltstone|23411|6|Mentioned|Map Legend|||||||||
27596|Ulupa Siltstone|23804|6|Mentioned|p16 Fig.1|||||||||
27596|Ulupa Siltstone|23818|5|Briefly described|p73 Fig.27|Adelaidean|Adelaidean|Of the Brachina Formation. Max. thickness: 4000-5000 ft.||||||
27596|Ulupa Siltstone|24176|5|Briefly described|p14, p24. Tb. 1|Adelaidean|Adelaidean|Basal pale green shale, intertongues with Brachina Formation.  Age is Marinoan.  Geological Province: Mount Painter Province.||||||14-MAY-07
27596|Ulupa Siltstone|24195|6|Mentioned|p44|||Lateral equivalent of the Brachina Formation||||||
27596|Ulupa Siltstone|24321|5|Briefly described|Map legend|Late Adelaidean|Late Adelaidean|Of the Wilpena Group.||||||14-MAY-07
27596|Ulupa Siltstone|24364|6|Mentioned|p29 Fig.3|Neoproterozoic|Neoproterozoic|||||||
27596|Ulupa Siltstone|24546|5|Briefly described|p2 - 3 Fig.2|Neoproterozoic|Neoproterozoic|Of Wilpena Group. Geological Province: Adelaide Fold Belt.||||||16-JAN-08
27596|Ulupa Siltstone|24586|6|Mentioned|p53|||Clastic sediments.  Overlies Nuccaleena Formation.  Geological Province: Adelaide Geosyncline.||||||
27596|Ulupa Siltstone|29778|6|Mentioned|p167|||||||||
27596|Ulupa Siltstone|29780|4|Described|p103|||||||||
27596|Ulupa Siltstone|30176|6|Mentioned|Map legend|Adelaidean|Adelaidean|Marinoan||||||
27596|Ulupa Siltstone|30177|4|Described|p89|||||||||
27596|Ulupa Siltstone|30261|6|Mentioned|Table 1|||Marinoan age||||||
27596|Ulupa Siltstone|30798|6|Mentioned|p116|||||||||
27596|Ulupa Siltstone|30801|6|Mentioned|p5|||Marinoan. Table P5-6||||||
27596|Ulupa Siltstone|30802|6|Mentioned|p12|||||||||
27596|Ulupa Siltstone|30807|6|Mentioned|p102|||Suggested map symbol||||||
27596|Ulupa Siltstone|32146|6|Mentioned|Fig.3|||||||||
27596|Ulupa Siltstone|32547|6|Mentioned|Fig.2|||Marinoan||||||
27596|Ulupa Siltstone|32724|6|Mentioned|Fig.1|||Marinoan. Correlation||||||
27596|Ulupa Siltstone|34535|5|Briefly described|p74|||||||||
27596|Ulupa Siltstone|34536|6|Mentioned|Map legend|Adelaidean|Adelaidean|Marinoan||||||
27596|Ulupa Siltstone|34812|6|Mentioned|p137|||||||||
27596|Ulupa Siltstone|35255|6|Mentioned|p15|||||||||
27596|Ulupa Siltstone|35356|6|Mentioned|p30|||||||||
27596|Ulupa Siltstone|35586|6|Mentioned|p26|||Suggested name to be abandoned.||||||
27596|Ulupa Siltstone|36126|6|Mentioned|Fig.1|||||||||
27596|Ulupa Siltstone|37461|6|Mentioned|Table 5.I|||||||||
27596|Ulupa Siltstone|37627|6|Mentioned|p188|||||||||
27596|Ulupa Siltstone|38110|6|Mentioned|p3|||||||||
27596|Ulupa Siltstone|38157|6|Mentioned|Table V|||See also Table XI.||||||
27596|Ulupa Siltstone|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Marinoan||||||
27596|Ulupa Siltstone|39352|6|Mentioned|Map legend|Adelaidean|Adelaidean|Marinoan||||||
27596|Ulupa Siltstone|40442|6|Mentioned|p10|||||||||
27596|Ulupa Siltstone|41429|3|Fully described|p223|||||||||
27596|Ulupa Siltstone|41500|6|Mentioned|Fig.1 P75|||||||||
27596|Ulupa Siltstone|42098|5|Briefly described|p54|||||||||
27596|Ulupa Siltstone|42222|6|Mentioned|Table 1 P4|||||||||
27596|Ulupa Siltstone|42241|5|Briefly described|p178|||||||||
27596|Ulupa Siltstone|42272|6|Mentioned|p403|||||||||
27596|Ulupa Siltstone|42542|5|Briefly described|Fig. 2a P11|||||||||
27596|Ulupa Siltstone|42720|5|Briefly described|map legend|Marinoan||||||||
27596|Ulupa Siltstone|42813|5|Briefly described|p22|||Of the Wilpena Group.||||||14-MAY-07
27596|Ulupa Siltstone|43052|5|Briefly described|p192,table 6.1|||Of the Wilpena Group.||||||14-MAY-07
27596|Ulupa Siltstone|44133|5|Briefly described|p50, 54|Adelaidian|Adeladian|||||||
27596|Ulupa Siltstone|44659|5|Briefly described|map legend|||Marinoan, lithology.||||||
27596|Ulupa Siltstone|44690|4|Described|map legend|||Geol. Atlas Series. (I/54-5). Unit of Wilpena Group. Marinoan.||||||
27596|Ulupa Siltstone|61238|4|Described|p46 Fig. 2, p47 Fig. 3|Neoproterozoic|Neoproterozoic|Of the Wilpena Group. Siltstone; shale, green-grey and purple.||||||14-MAY-07
27596|Ulupa Siltstone|63458|6|Mentioned|p897 Fig.19. |Ediacaran|Ediacaran|||Unit in Wilpena Group.||||
27596|Ulupa Siltstone|67030|4|Described|p407-15|Ediacaran|Ediacaran|Paleo-magnetic information presented. Best age estimate of ~590 Ma by inference from Brachina Formation. Pole position is very similar to the Black Hill Norite.|590 Ma|||Equivalent to the Brachina Formation; overlies the Nuccaleena Formation.||26-APR-12
27596|Ulupa Siltstone|68030|6|Mentioned|p237|Ediacaran|Ediacaran|Flinders Ranges. Correlative of Brachina Formation to the N and E.|||||Green and grey fine-grained siltstone.|
27596|Ulupa Siltstone|68271|5|Briefly described|p695|||Adelaide Rift Complex.||||Overlain unconformably by Wonoka Formation. Underlain by Nuccaleena Formation.||
27596|Ulupa Siltstone|69019|4|Described|p54-56, p152.|Neoproterozoic|Neoproterozoic|Defined by Mirams (in Thomson et al.,1964). Type section is ~10 km NE of Mt. Bryan where it is ~1,500 m thick (elsewhere up to ~5,000 m). Has a high magnetic response.||Unit in Sandison Subgroup.||Equivalent to Brachina Formation. Is overlain by Bunyeroo Formation and Burr Well Member (Wonoka Formation).|Monotonous succession of finely laminated grey-green siltstone, sandstone; local small dolomite lenses.|
27596|Ulupa Siltstone|70031|6|Mentioned|p246|||||||||
27596|Ulupa Siltstone|70384|5|Briefly described|Map legend.|Ediacaran|Neoproterozoic|Adelaide Geosyncline.||Of Sandison Subgroup.|||Monotonous sequence of finely-laminated siltstone; grey-green coarse middle sequence; siltstone and fine sandstone (+/- local small dolomite lenses) are distinguished in more complete northern sections.|23-JAN-19
27596|Ulupa Siltstone|70406|4|Described|p126, p125|||Type section defined by Mirams (1964) near Mount Bryan, Burra map sheet. Three of same members (lithofacies) as Brachina Formation recognised by Plummer(1978), but are time-transgressive distal equivalents, so Ulupa Siltstone name retained.|||||Succession of green, grey and locally purple shales.|
27596|Ulupa Siltstone|70407|5|Briefly described|p107, 108|||||||Unconformably overlain by Wilcolo Sandstone on the south limb of Mt Goddard Syncline?||
27596|Ulupa Siltstone|71237|14|Not recorded|p9, 18|||||||||
27596|Ulupa Siltstone|71241|6|Mentioned|p13, p9|||Burra sheet area.||||Brachina Formation equivalent.||
27596|Ulupa Siltstone|72456|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Marree 1:250k map sheet. |||||Siltstone, shale, green-grey and purple.|
27596|Ulupa Siltstone|73093|5|Briefly described|map legend|Neoproterozoic|Neoproterozoic||||||Siltstone; shale, green-grey and purple.|09-DEC-21
33650|Umutju Granite Suite|24301|6|Mentioned|p37 Appendix 1|||||||||
33650|Umutju Granite Suite|60572|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Includes the Mantapyika and Puka Granites.  Age: ~1180-1120Ma.  Geological Province: Musgrave Block.||||||
33650|Umutju Granite Suite|60683|2|Defined|p55 Appendix, p14|Mesoproterozoic|Mesoproterozoic|Includes Mantapayika, Puka and Walytjatjata Granites and unnamed charnockite and clinopyroxene granite.  Synonymous with part of Musgrave-Mann Metamorphics, Olia Gneiss and unnamed metamorphosed granites of Forman (1966a, 1972). See also p10 Tb.1, p42-43.||||||
33650|Umutju Granite Suite|61386|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Includes the Walytjatjata, Puka and Mantapayika Granites. Age: ~1180-1120Ma. Geological Province: Musgrave Block.||||||19-OCT-05
33650|Umutju Granite Suite|69091|6|Mentioned|p103 Fig.5.6|||||||||
33650|Umutju Granite Suite|70793|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Geological province: Paterson Orogen, Musgrave Province. Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma); Giles Event (1085-1040 Ma); Musgrave Orogeny (1220-1150 Ma). See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop14_lut.csv, 500k_interpgeop_lut.csv.|1175+\-10 Ma; 1148+\-6 Ma|Unit of Pitjantjatjara Supersuite.|||Medium- to coarse-grained hornblende-pyroxene(-garnet) metagranite|
33650|Umutju Granite Suite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||charnockite, migmatite, granite|
33650|Umutju Granite Suite|71268|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Geological Province: Paterson Orogen, Musgrave Province. Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma); Giles Event (1085-1040 Ma). See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 1m_geologyp12_lut.csv, 500k_interpgeop16_lut.csv.|1175+\-10 Ma; 1148+\-6 Ma|Unit of Pitjantjatjara Suite.|||Medium- to coarse-grained hornblende--pyroxene(--garnet) metagranite|
33650|Umutju Granite Suite|71592|5|Briefly described|Appendix A.|||Musgrave Province. Age determination by zircon Pb-Pb evaporation.|1172+/-6 Ma (crystallisation).||||Granite.|
33650|Umutju Granite Suite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoproterozoic|Mesoproterozoic|Musgrave Province, Paterson Orogen.|Max age 1175+/-10 Ma, Min 1148+/-6 Ma.|Pitjantjatjara Supersuite|||Medium- to coarse-grained hornblende-pyroxene(-garnet) metagranite.|
79175|Undawidgi Supersuite|70831|5|Briefly described|p25-p26|Calymmian|Calymmian|Coompana Province. Misspelt as the Undawidji Supersuite on p25.|c. 1505-1487 Ma|||||
79175|Undawidgi Supersuite|71143|5|Briefly described|p427,429,431-432,434,434,440|Calymmian|Calymmian|Geological province: Coompana Province. Alkali-calcic to alkalic, high-K to shoshonitic suite. Transitional A-type felsic rocks with a crustal source component that was primitive and likely hydrated and oxidised  (contains juvenile isotope values consistent with extensional processes involving asthenospheric input). May reflect recycling of c. 1600 Ma arc crust of the Toolgana Supersuite, with additional but variable juvenile mantle input (Smithies et al., 2015b).|c. 1490 Ma|||||
79175|Undawidgi Supersuite|71165|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Western Coompana Province.|c.1490 Ma.|||Is intruded by Moodini Supersuite.|Foliated metagranite and felsic metavolcanic rocks.|
79175|Undawidgi Supersuite|71891|5|Briefly described|p7|||Coompana Province.|c. 1490 Ma||||Metagranitic and possibly bimodal metavolcanic rocks. Variably foliated metatonalites and metamonzogranites, metamonzodiorites and variably sheared/mylonitic felsic and mafic schists.|
79175|Undawidgi Supersuite|72242|5|Briefly described|p27,31|Calymmian|Calymmian|Geological province: Coompana Province. A-type magmatism, post-dating Kararan Orogeny. |c. 1505-1487 Ma||||Granitic gneiss.|
79175|Undawidgi Supersuite|72344|5|Briefly described|p3, p5-p7, p9, p61, p63, p71|Calymmian|Calymmian|Coompana Province. Rift related and interpreted to include recycled Toolgana Supersuite material. Similar in age to the granodiorite gneiss from Mallabie 1 drillhole. Ages are derived from Fraser and Neumann, 2016 and Wingate et al, 2015a. See also p143.|1487-1526 Ma (SHRIMP U-Pb)||Includes the Gilgerabbie Suite and Bunburra Suite.||Metagranitic and possible bimodal metavolcanic rocks including variably foliated metatonalites and metamonzogranites, which are locally gneissic and migmatitc, metamonzodiorites and variably sheared/mylonitic felsic and mafic schists.|04-SEP-19
79175|Undawidgi Supersuite|72465|5|Briefly described|p4, 10|||Coompana Province. Extension and rift-related; derived by melting of lower mafic crust and a mantle component. Underwent metamorphism 1174 +/- 12 Ma.|1505 +/- 7 Ma to 1487 +/- 9 Ma.||||Variably foliated metatonalites and metamonzogranites, locally gneissic and migmatitic; metamonzodiorites; and variably sheared/mylonitic felsic and mafic schists (of monzogranitic or volcanic protolith).|
79175|Undawidgi Supersuite|72466|5|Briefly described|p4, 10|||Basement to Coompana Province. Extension and rift-related; rocks derived from melting of lower mafic crust, recycled Toolgana Supersuite material, and introduction of a mantle component. Metamorphosed at 1174 +/- 12 Ma.|1613/- 13 Ma to 1591 +/- 11 Ma.||||Variably foliated metatonalites and metamonzogranites, locally gneissic and migmatitic; metamonzodiorites; and variably sheared/mylonitic felsic and mafic schists (the former with ?monzogranitic or volcanic protolith).|
79175|Undawidgi Supersuite|72467|5|Briefly described|p4, 10|||Coompana Province. Extension and rift-related; derived by melting of lower mafic crust and a mantle component. Underwent metamorphism 1174 +/- 12 Ma.|1505 +/- 7 Ma to 1487 +/- 9 Ma.||||Variably foliated metatonalites and metamonzogranites, locally gneissic and migmatitic; metamonzodiorites; and variably sheared/mylonitic felsic and mafic schists (of monzogranitic or volcanic protolith).|
79175|Undawidgi Supersuite|72468|5|Briefly described|p4, p10|Calymmian|Calymmian|Coompana Province. Derived by melting of lower mafic crust and the introduction of a mantle component. Also interpreted to include recycled Toolgana Supersuite material. Magmatic ages include 1505 +/- 7 Ma, 1499 +/- 9 Ma, 1488 +/- 4 Ma, and 1487 +/- 9 Ma. Metamorphic age of 1174 +/- 12 Ma.|c. 1500-1490 Ma||||Metagranitic and possible bimodal metavolcanic rocks including variably foliated metatonalites and metamonzogranites, which are locally gneissic and migmatitic; metamonzodiorites; and variably sheared/mylonitic felsic and mafic schists.|
79175|Undawidgi Supersuite|72469|5|Briefly described|p4, p10|Calymmian|Calymmian|Coompana Province. Derived by melting of lower mafic crust and the introduction of a mantle component. Also interpreted to include recycled Toolgana Supersuite material. Magmatic ages include 1505 +/- 7 Ma, 1499 +/- 9 Ma, 1488 +/- 4 Ma, and 1487 +/- 9 Ma. Metamorphic age of 1174 +/- 12 Ma.|c. 1500-1490 Ma||||Metagranitic and possible bimodal metavolcanic rocks including variably foliated metatonalites and metamonzogranites, which are locally gneissic and migmatitic; metamonzodiorites; and variably sheared/mylonitic felsic and mafic schists.|
79175|Undawidgi Supersuite|72470|5|Briefly described|p4, p10|Calymmian|Calymmian|Coompana Province. Derived by melting of lower mafic crust and the introduction of a mantle component. Also interpreted to include recycled Toolgana Supersuite material. Magmatic ages include 1505 +/- 7 Ma, 1499 +/- 9 Ma, 1488 +/- 4 Ma, and 1487 +/- 9 Ma. Metamorphic age of 1174 +/- 12 Ma.|c. 1500-1490 Ma||||Metagranitic and possible bimodal metavolcanic rocks including variably foliated metatonalites and metamonzogranites, which are locally gneissic and migmatitic; metamonzodiorites; and variably sheared/mylonitic felsic and mafic schists.|
79175|Undawidgi Supersuite|72471|5|Briefly described|p4, p10|Calymmian|Calymmian|Coompana Province. Derived by melting of lower mafic crust and the introduction of a mantle component. Also interpreted to include recycled Toolgana Supersuite material. Magmatic ages include 1505 +/- 7 Ma, 1499 +/- 9 Ma, 1488 +/- 4 Ma, and 1487 +/- 9 Ma. Metamorphic age of 1174 +/- 12 Ma.|c. 1500-1490 Ma||||Metagranitic and possible bimodal metavolcanic rocks including variably foliated metatonalites and metamonzogranites, which are locally gneissic and migmatitic; metamonzodiorites; and variably sheared/mylonitic felsic and mafic schists.|
79175|Undawidgi Supersuite|72472|5|Briefly described|p4, p10|Calymmian|Calymmian|Coompana Province. Derived by melting of lower mafic crust and the introduction of a mantle component. Also interpreted to include recycled Toolgana Supersuite material. Magmatic ages include 1505 +/- 7 Ma, 1499 +/- 9 Ma, 1488 +/- 4 Ma, and 1487 +/- 9 Ma. Metamorphic age of 1174 +/- 12 Ma.|c. 1500-1490 Ma||||Metagranitic and possible bimodal metavolcanic rocks including variably foliated metatonalites and metamonzogranites, which are locally gneissic and migmatitic; metamonzodiorites; and variably sheared/mylonitic felsic and mafic schists.|
79175|Undawidgi Supersuite|72934|5|Briefly described|p2, p4, p12, App.A|Calymmian|Calymmian|Geochemically and temporally similar to the Gilgerabbie Suite. Associated with, but slightly postdates Bunburra Suite magmatism. Possibly reflects recycling of c. 1600 Ma arc crust of the Toolgana Supersuite with additional mantle input.|c. 1490 Ma||||Metamorphosed syenogranite, monzogranite, tonalite, monzodiorite, syenite, and felsic volcanic rocks.|
79175|Undawidgi Supersuite|72947|5|Briefly described|p4, p7-9, p11, p13|Calymmian|Calymmian|Coompana Province. Derived by melting of lower mafic crust with mantle input during lithospheric extension.|c. 1500 Ma / 1505 - 1487 Ma||Gilgerabbie Suite||A-type rocks.|
79175|Undawidgi Supersuite|73084|4|Described|p: 12, 15, ~38-47, 69-70, 72-73...|Calymmian|Calymmian|Coompana Province. A-type or transitional A-type; greenschist to lower amphibolite facies. Significant crustal source component and parts with an upwelled asthenospheric mantle component. Similar rocks were intersected in the Mallabie 1 drillcore in SA. Slightly younger than the Bunburra Suite. Report includes lithologic/petrographic description, structural analysis, whole-rock geochemistry, geochronology, Sm-Nd, Lu-Hf. Also p: ~101-117, 123-125, 128, 133-135, 142.42.|1499-1479 Ma)||||Metagranites including metamonzogranites, metamonzodiorite and metasyenite. Also contains mafic schist and a grey schist interpreted as a metarhyolite. Includes porphyritic monzogranite gneiss interlayered with the metatonalite, metasyenogranite.|
79175|Undawidgi Supersuite|73091|5|Briefly described|map legend|Calymmian|Calymmian||C. 1500-1530 Ma||Includes the Gilgerabbie Suite.||Granitic gneiss.|30-NOV-21
79175|Undawidgi Supersuite|73224|5|Briefly described|p42, p44|Calymmian|Calymmian|Coompana Province, western. A-type. Product of intracontinental extension following cessation of subduction. Represents recycling of the c. 1600 Ma arc crust with additional juvenile mantle input.|c. 1505-1487 Ma||Gilgerabbie Suite|||
79175|Undawidgi Supersuite|73225|5|Briefly described|p3, 4, 18, p22 Fig.10|||Coompana Province. West of the Mulyawarra Shear Zone. Formed by recycling of c.1600 Ma arc crust, with additional juvenile mantle input,  in a rift setting.|c.1505-1487 Ma.||Gilgerabbi Suite||Bimodal; A-type.|
79175|Undawidgi Supersuite|73641|6|Mentioned|p4||||||Gilgerabbie Suite|||
23088|Ungoolya Group|22746|4|Described|Fig.3 p515, p521|Neoproterozoic III|Neoproterozoic III|Segregated into a lower (4300m) and upper group||||||
23088|Ungoolya Group|22802|6|Mentioned|p872|||Officer Basin||||||
23088|Ungoolya Group|22901|5|Briefly described|78|||Geol province Officer Basin.||||||30-SEP-08
23088|Ungoolya Group|22922|5|Briefly described|34|||||||||
23088|Ungoolya Group|23282|4|Described|p59|||Was 'Ungoolya Formation' of Dunster (1987), then changed informally to Ungoolya Group by Sukanta (1993), then formally defined by Zang (1995). Also previously Rodda beds of Brewer (1987), and in part the Wright Hill beds of Major (1973). of Officer Basin.||||||18-APR-06
23088|Ungoolya Group|23287|6|Mentioned|p104|||of Officer Basin.||||||
23088|Ungoolya Group|23479|5|Briefly described|p26|||Geological Province: Gawler Craton.||||||
23088|Ungoolya Group|23524|5|Briefly described|p221 Fig. 3|Neoproterozoic|Neoproterozoic|||||||
23088|Ungoolya Group|23557|5|Briefly described|p95 Fig.1|Neoproterozoic III|Neoproterozoic III|Geological Province: Officer Basin.||||||
23088|Ungoolya Group|24112|5|Briefly described|p254 Fig.2|Neoproterozoic|Neoproterozoic|Geological Province: Officer Basin||||||
23088|Ungoolya Group|43657|6|Mentioned|p3||Neoproterozoic|||||||
23088|Ungoolya Group|43690|6|Mentioned|Fig.2,p157||Neoproterozoic|||||||
23088|Ungoolya Group|43743|6|Mentioned|Fig.2,p33||Neoproterozoic|||||||
23088|Ungoolya Group|44109|5|Briefly described|p22 Fig. 19|Neoproterozoic|Neoproterozoic|Includes the Rodda beds. Geological Province: central Officer Basin.||||||
23088|Ungoolya Group|60565|6|Mentioned|p18|Neoproterozoic III|Neoproterozoic III|||||||
23088|Ungoolya Group|61732|5|Briefly described|p4 Fig. 3, p145 Fig. 51|Marinoan|Marinoan|Includes the Dey Dey Mudstone, Karlaya Limestone, Tanana Formation, Narana Formation Munyarai Formation and Punkerri Sandstone. Geological Province: central Officer Basin. The name Ungoolya occurs in SA.||||||07-FEB-11
23088|Ungoolya Group|62453|5|Briefly described|p5 Fig. 3|Ediacaran|Ediacaran|Geological Province: Officer Basin.||||||
23088|Ungoolya Group|62570|5|Briefly described|p579, p580 Figs. 2 and 3|Neoproterozoic|Neoproterozoic|Unconformably overlain by Relief Sandstone (Marla Group). Acritarch-bearing unit. Geological Province: Officer Basin.||||||10-AUG-07
23088|Ungoolya Group|63397|2|Defined|28|Neoproterozoic III|Neoproterozoic III|Type section in text. Max Thickness: 4000m. Mainly siltstone and silty mudstone, with limestone and dolomite and minor sandstone. Overlies the Murnaroo Formation.||||||18-JUL-07
23088|Ungoolya Group|63811|5|Briefly described|p499-500, 502-5, 519-528 App A|Ediacaran|Ediacaran|Previously Rodda beds, in the Giles 1 drill hole, Eastern Officer Basin. Correlated with Doushantuo Formation, South China.|||Includes Dey Dey Mudstone, Karlaya Limestone and Tanana Formation.|Overlies Lake Maurice Group.||28-MAR-12
23088|Ungoolya Group|64103|6|Mentioned|p400 Fig. 3|Ediacaran|Ediacaran|Geological Province: Officer Basin.||||||07-FEB-11
23088|Ungoolya Group|64724|5|Briefly described|p49 Fig. 7|Ediacaran|Ediacaran|Deposited in the Amadeus Basin during the Centralian 3 event (~600-544 Ma)||||||
23088|Ungoolya Group|64794|5|Briefly described|p235-245,p248-253,p255,p265-266,p269-275|Ediacaran|Ediacaran|Of Officer Basin. Formerly named Rodda Beds. Marine deposits, described in detail.|~580-550 Ma.||Narana Formation, Tanana Formation, Munyarai Formation, Dey Dey Mudstone, Karlaya Limestone.|||
23088|Ungoolya Group|64970|6|Mentioned|p719 Fig. 2|Neproterozoic|Neoproterozoic|Geological Province: Officer Basin.||||||27-MAY-09
23088|Ungoolya Group|65365|5|Briefly described|p10 Fig. 4|Ediacaran|Ediacaran|Eastern Officer Basin. Includes Acanthomorph acritarchs.||||||
23088|Ungoolya Group|65366|5|Briefly described|p23 Fig. 3|Ediacaran|Ediacaran|Eastern Officer Basin. Includes Acanthomorph acritarchs.||||||
23088|Ungoolya Group|66569|5|Briefly described|p861 fig.2,|Ediacaran|Ediacaran|Officer Basin. Informally split into Upper and Lower sections; includes Narana, Munyarai and Tanana Formations, Karlaya Limestone, Dey Dey Mudstone. Overlies Murnaroo Sandstone unconformably.||||||
23088|Ungoolya Group|67120|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic||||||Mudstone, siltstone, limestone, calcareous siltstone, sandstone, dolomite, conglomerate.|
23088|Ungoolya Group|67536|6|Mentioned|Map Legend|||One of several Formations mapped collectively as N2.|||||Dominantly marine shale, siltstone, sandstone and limestone.|
23088|Ungoolya Group|67912|5|Briefly described|p12-13, 23, 25-27|Ediacaran|Ediacaran|Officer Basin. Previously part of the Rodda beds. 220.1m thick in Lake Maurice West 1 drillhole.|||Dey Dey Mudstone, Karlaya Limestone, Tanana Formation.|Overlies Murnaroo Formation. Is overlain by Observatory Hill Formation.||
23088|Ungoolya Group|67921|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Shown only in section and grouped with Punkerri Sandstone, Rodda beds - possibly previous name for Ungoolya Group. Group description: Marine sandstone, grey indurated mudstone and limestone.|||Includes Karlaya Limestone, Wright Hill beds|Said to be equivalent to Wilpena Group||
23088|Ungoolya Group|68269|6|Mentioned|p673-674|Ediacaran|Ediacaran|Officer Basin. Lower and upper portions are mentioned.|||Narana Formation, Munyarai Formation, Tanana Formation, Karlaya Limestone, Dey Dey Mudstone|Underlain by Murnaroo Sandstone.||
23088|Ungoolya Group|68270|5|Briefly described|p683|Ediacaran|Ediacaran|Eastern Officer Basin.||||Underlain by Lake Maurice Group.||
23088|Ungoolya Group|69003|6|Mentioned|p60|Ediacaran|Ediacaran|E Officer Basin.||||||
23088|Ungoolya Group|69946|6|Mentioned|p38|||||||Is unconformably overlain by Relief Sandstone.||
23088|Ungoolya Group|70336|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic||||||Mudstone, siltstone, limestone, calcareous siltstone, sandstone, dolomite, conglomerate.|
23088|Ungoolya Group|71268|5|Briefly described|1m_geologyp12_lut.csv||||||Includes Punkerri Sandstone.|||
23088|Ungoolya Group|71342|6|Mentioned|Ch5 p38|Adelaidean|Adelaidean|Arckaringa Basin. ||||Unconformably overlain by the Relief Sandstone.|Volcanics.|
23088|Ungoolya Group|72476|6|Mentioned|p26, p36 Fig.9|||Officer Basin. Sediments derived from the Musgrave Block.||||||
23088|Ungoolya Group|72478|5|Briefly described|p8|Marinoan|Marinoan|Officer Basin.|c. 600-545 Ma||Includes the Dey Dey Mudstone, Karlaya Limestone, Tanana Formation, Narana Formation, Munyarai Formation, Punkerri Sandstone.|Unconformably underlies Marla Group. Overlies the Lake Maurice Group.||24-MAR-21
23088|Ungoolya Group|73099|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Officer Basin.|||Dey Dey Mudstone, Karlaya Limestone, Tanana and Narana Formations.|Overlies Lake Maurice Group. Is overlain by Marla Group.||
23088|Ungoolya Group|73100|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Subsurface. Appears as UNGOOLYA GROUP (RODDA BEDS).||||Equivalent to Wilpena Group.||
23088|Ungoolya Group|73109|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Subsurface. Also referred to as Rodda beds.|||Karlaya Limestone.|Equivalent to Wilpena Group.||
23088|Ungoolya Group|73111|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Subsurface. Appears as UNGOOLYA GROUP (RODDA BEDS).|||Karlaya Limestone.|Equivalent to Wilpena Group.||
31400|Upalinna Subgroup|22510|2|Defined|table1p37,41|||Early Marinoan in age. Disconformably overlies the Nepouie Subgroup; mostly disconformably overlain by the Yerelina Subgroup. Rb/Sr maximum depositional age: 724+/-40Ma (Webb and Coats, 1980).  Type section: As for the constituent formations. A useful reference section is along the Oraparinna and Enorama Creeks, from 138degrees42'40"E, 31degrees21'43"S to 138degrees38'14"E,31degrees19'57"S. Max. thickness: >2000m||||||26-NOV-22
31400|Upalinna Subgroup|23477|5|Briefly described|p49 Fig 3|Neoproterozoic|Neoproterozoic|Geological Province: Curnamona Province.||||||
31400|Upalinna Subgroup|24546|5|Briefly described|p2 - 3 Fig.2|Neoproterozoic|Neoproterozoic|Of Umberatana Group. Geological Province: Adelaide Fold Belt.||||||16-JAN-08
31400|Upalinna Subgroup|60718|5|Briefly described|p49 Fig. 2|Adelaidean|Adelaidean|Geological Province: Adelaide Geosyncline.||Of Umberatana Group.|Includes Elatina, Amberoona and Yankaninna Formations.|||15-APR-11
31400|Upalinna Subgroup|60953|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Of the Umberatana Group.||||||27-APR-05
31400|Upalinna Subgroup|60959|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Of the Umberatana Group.||||||
31400|Upalinna Subgroup|61108|5|Briefly described|map legend|Adelaidean|Adelaidean|Of the Umberatana Group. Mainly interglacial. Marine and marginal marine siltstone and sandstone; oolitic, sandy and stromatolitic limestone.||||||06-JUN-05
31400|Upalinna Subgroup|61238|5|Briefly described|p44 Fig. 1|Neoproterozoic|Neoproterozoic|Of the Umberatana Group.||||||13-FEB-08
31400|Upalinna Subgroup|61732|5|Briefly described|p28 Fig. 13|Marinoan|Marinoan|Of the Umberatana Group. Includes Sutherland, Etina and Angepena Formations, and Tarcowie Siltstone; and Waukaringa Siltstone, Enorama Shale, Wilmington, Trezona and Yaltipena Formations. Geol Prov: Adelaide Rift Complex.||||||07-FEB-11
31400|Upalinna Subgroup|62085|6|Mentioned|p19 Fig.4|Cryogenian|Cryogenian|||Unit in Umberatana Group.|||Siltstone, sandstone, limestone.|
31400|Upalinna Subgroup|62592|5|Briefly described|p20 Fig.2.4, p50 Table 5.1, pp58-59.|Marinoan|Marinoan|Colour scheme shown for interpretation of Curnamona seismic sections. Written as SubGroup.||Unit in Umberatana Group.|Includes Sunderland, Etina, Trezona and Yaltipena Formations and Enorama Shale.||Basal conglomerate grading upwards into redbeds and carbonates.|
31400|Upalinna Subgroup|62724|5|Briefly described|p16 Fig. 2|Neoproterozoic|Neoproterozoic|Siltstone, sandstone, limestone, conglomerate. Geological Province: Curnamona Province.||||||07-FEB-11
31400|Upalinna Subgroup|62903|6|Mentioned|p730 Fig.1|||Adelaide Rift Complex.||||is overlain by Yerelina Subgroup||
31400|Upalinna Subgroup|63102|5|Briefly described|p8|Neoproterozoic|Neoproterozoic|Geological province: Curnamona Province.|||||Siltstone, sandstone, limestone, conglomerate.|
31400|Upalinna Subgroup|64846|5|Briefly described|p198|Cryogenian|Cryogenian|Interglacial succession.||Of the Umberatana Group.|Includes Enorama Shale, Amberoona Formation and Yankaninna Formation.|||
31400|Upalinna Subgroup|65493|5|Briefly described|p910, p909 Fig 2|Cryogenian|Cryogenian|Of the Umberatana Group. Unconformably overlies the Nepouie Subgroup. Includes Yankannina Formation, Amberoona Formation, Enorama Shale. Interglacial deposit.||||||
31400|Upalinna Subgroup|67180|4|Described|p600, p601 Fig.1, p602 Fig.2|Cryogenian|Cryogenian|Marinoan Age. Defined by Preiss et al. 1998. ||Unit in Umberatana Group|Includes Enorama Shale, Amberoona Formation, Weetootla Dolomite Member, Yankaninna Formation|Overlies the Nepouie Subgroup.||
31400|Upalinna Subgroup|67870|5|Briefly described|p9|Neoproterozoic|Neoproterozoic|Adelaide Rift System.||Umberatana Group.|Includes Angepena Formation.|||23-JAN-19
31400|Upalinna Subgroup|67979|4|Described|p528, p531 Fig.2, p542, 543-545|Marinoan||Interglacial succession (Preiss et al. 1998). Nepouie-Upalinna Subgroup boundary now proposed to coincide with the Sturtian-Marinoan Series boundary in northern & central Flinders Ranges, on basis of new correlations.||Umberatana Group||Overlies Nepouie Subgroup; is overlain by Yerelina Subgroup.||22-SEP-14
31400|Upalinna Subgroup|68068|5|Briefly described|Map legend|Marinoan|Marinoan|Adelaide Geosyncline.||Unit in Umberatana Group.|Includes Yankaninna and Amberoona Formations.|||
31400|Upalinna Subgroup|68269|6|Mentioned|p674|Cryogenian|Cryogenian||||Marino Arkose Member|||
31400|Upalinna Subgroup|69019|4|Described|p41, p49-51.|Neoproterozoic|Neoproterozoic|Of Preiss et al. (1998) in a revision of the Umberatana Group. Early Marinoan. Has 12 Formations; 2 in this map area.||Unit in Umberatana Group.|Includes Yankaninna and Amberoona Formations.||Two transgressive-regressive sequences of siltstone, sandstone, limestone, dolomite and sandy limestone.|
31400|Upalinna Subgroup|69023|5|Briefly described|p64, p67, p70-72|Neoproterozoic|Neoproterozoic|Defined by Preiss et al. (1998). Marinoan age. Represents two transgressive-regressive sequences of siltstone, sandstone, limestone, dolomite and sandy limestone.||Unit in Umberatana Group.|Includes Yankaninna and Amberoona Formations.|||
31400|Upalinna Subgroup|70031|5|Briefly described|p245|Cryogenian|Cryogenian|Adelaide Geosyncline. Entirely comprises interglacial successions recording overall lowering of sea level at the waning stages of the Sturtian glaciation.||Unit of Umberatana Group.|Includes Trezona Formation, Enorama Shale, Etina Formation and Angepena Formation.|Overlain unconformably by Yerelina Subgroup/Elatina Formation. Underlain by Nepouie Subgroup/Brighton Limestone.|Coarse to fine-grained clastics interbedded by carbonates.|
31400|Upalinna Subgroup|70334|5|Briefly described|p20,23,47,51|Neoproterozoic|Neoproterozoic|Geological province: Gawler Craton. Of Adelaide Geosyncline and Stuart Shelf. ||Unit of Umberatana Group.|Includes Wilmington Formation and Angepena Formation.|||
31400|Upalinna Subgroup|70384|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Adelaide Geosyncline. Age shown more specifically as Marinoan [Cryogenian].||Of Umberatana Group.|Includes Yankaninna, Angepena, Amberoona, Trezona Formations; Enorama Shale.|Unconformably overlies Nepouie Subgroup. Is overlain unconformably by Yerelina Subgroup.||23-JAN-19
31400|Upalinna Subgroup|70405|6|Mentioned|p14 figure 6|Neoproterozoic|Neoproterozoic||||||Siltstone, sandstone, limestone and conglomerate.|
31400|Upalinna Subgroup|70657|5|Briefly described|p9 Fig.3|Neoproterozoic|Neoproterozoic||||||Siltstone, sandstone, limestone, conglomerate.|
31400|Upalinna Subgroup|70658|6|Mentioned|p14|Neoproterozoic|Neoproterozoic||||||Siltstone, sandstone, limestone, conglomerate.|
31400|Upalinna Subgroup|70865|6|Mentioned|p2|||Adelaide Hills area.||||||
31400|Upalinna Subgroup|71037|5|Briefly described|p22-23 Fig.2, p27 Fig.6|Neoproterozoic|Neoproterozoic|Shown  on the Six Mile Hill 1:75,000 surface geology map (p22-23 Fig.2) and Interpreted bedrock geology (p27 Fig.6). Age shown as Marinoan.||Umberatana Group||Shown as older than Tent Hill Formation, Wilpena Group and younger than Tapley Hill Formation. Subgroup with Yerelina Subgroup.|Sandstone, siltstone and conglomerate.|
31400|Upalinna Subgroup|71129|4|Described|p1,15,107,109,111,118,126|Cryogenian|Cryogenian|Of Stuart Shelf. Deposited during ensuing glacio-eustatic sea-level rise after Sturt Glaciation. Clastic sedimentation in a shallowing rift during Marinoan Epoch, deposited in shallow marine to supratidal environment. See also p,184,187,208,225,227.||Unit of Umberatana Group.|Includes Augusta Shale and Yudnapinna Beds.|Overlies the Nepouie Subgroup. Overlain by the Yerelina Subgroup.|Sandstone, siltstone and conglomerate; undifferentiated.|13-NOV-19
31400|Upalinna Subgroup|71130|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|||Umberatana Group.|||Sandstone, siltstone and conglomerate.|
31400|Upalinna Subgroup|71131|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|||Umberatana Group.|||Sandstone, siltstone and conglomerate.|
31400|Upalinna Subgroup|71895|6|Mentioned|APP4. p4, |||Punt Hill Region.||||||
31400|Upalinna Subgroup|72090|5|Briefly described|p34, p37|||Gawler Craton.|||||Moderate brown, fine-grained to gravel, poorly sorted, sub-angular to sub-rounded clasti-volcanics.|
31400|Upalinna Subgroup|73093|5|Briefly described|map legend|Neoproterozoic|Neoproterozoic||||||Siltstone and sandstone; sandy, intraclastic and stromatolitic limestone and dolomite.|09-DEC-21
31400|Upalinna Subgroup|73107|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Adelaide Geosyncline.|||||Undifferentiated: grey andalusite schist and metasiltstone.|
31400|Upalinna Subgroup|73188|5|Briefly described|p316, p326|Neoproterozoic|Neoproterozoic|Mount Lofty Ranges.||Umberatana Group|Wilmington Formation, Angepena Formation|||
31400|Upalinna Subgroup|73236|6|Mentioned|p36, p38|Cryogenian|Cryogenian|Marine sedimentary rocks.||Umberatana Group, Heysen Supergroup|Wilmington Formation, Marino Arkose Member, Angepena Formation|Underlain by Brighton Limestone (Nepouie Subgroup). Overlain by Elatina Formation (Yerelina Subgroup).||
31400|Upalinna Subgroup|74367|5|Briefly described|p3, p7 Fig.6, p8, p19, p22|Cryogenian|Cryogenian|Previously part of the now superseded 'Willochra Subgroup'.||Umberatana Group|Brighton Limestone, Cox Sandstone Member, Tarcowie Siltstone, Wilmington Formation, Enorama Shale, Amberoona Formation, Trezona Formation, Yaltipena Formation|||
34655|Uraidla Phyllite Member|22869|2|Defined|p38, p45||Neoproterozoic|New name, interbed in the Arbury Park Sandstone Member, correlates with interbeds in the Rhynie Sandstone||||||07-JUL-20
34655|Uraidla Phyllite Member|22889|5|Briefly described|p33|Adelaidean|Adelaidean|Parent - Aldgate Sandstone.  Tentatively identified as a deformed mafic tuff (Priess,1997), and is correlated with the Jarrold Basalt Member of the Rhynie Sandstone p33.||||||
83055|VC Coal|73167|6|Mentioned|p664 Fig. 2|Permian|Permian|Cooper Basin.||Patchawarra Formation [?]||||
83055|VC Coal|73244|6|Mentioned|p86|Permian|Permian|[Possibly an abbreviated name]. Cooper Basin. Associated with the Mid-Permian Event[?].||||||
83055|VC Coal|73343|6|Mentioned|p337|Permian|Permian|Cooper Basin.||Patchawarra Formation||Underlain by Moorari Beds.||
83055|VC Coal|73479|6|Mentioned|p156 Fig.2|Permian|Permian|Cooper Basin. Fluvio-deltaic/lacustrine/swamp depositional environment.||Patchawarra Formation||||
75705|Varavaranha Formation|70384|5|Briefly described|Map legend.|Proterozoic|Proterozoic|Included with Mesoproterozoic units but marked "?Age uncertain". Carries anomalous base-metal values at Parabarana Hill. Two other facies are mapped separately. One comprises calc-silicate-marble: marble, recrystallised with calc-silicate minerals; carries anomalous base-metal values and secondary copper mineralisation at Parabarana Hill; deformed and fragmented by the Paralana Fault and shear zone. The second comprises graphitic schist; quartz-sericite-graphite schist with irregular parallel veins containing quartz, K-feldspar, muscovite/sericite, graphite and tourmaline; not portrayed on the map as the surface extent has not been fully determined.||||Is intruded by Mount Neill and Box Bore Granites.|Banded calc-silicate gneiss: epidotised banded quartz-albite gneiss, containing many variously-orientated blocks, ?brecciated, near Parabarana Hill. Banding exhibits multiple deformation fabrics and refolded isoclinal folds.|
75705|Varavaranha Formation|75063|6|Mentioned|p94 Fig.2|||Northern Flinders Ranges area.||||||
81749|Venus Supersuite|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Southern Gawler Craton.|1577 +/- 7 Ma.|||||
25578|Victor Harbour Granite|23818|6|Mentioned|p107|||||||||
25578|Victor Harbour Granite|23996|4|Described|p352, p535 Fig.3|||Geological Province: Adelaide Fold Belt.||||||17-NOV-22
25578|Victor Harbour Granite|30381|6|Mentioned|p229|||||||||
25578|Victor Harbour Granite|33224|6|Mentioned|p54|||||||||
25578|Victor Harbour Granite|34612|6|Mentioned|p107|||||||||
25578|Victor Harbour Granite|38068|6|Mentioned|p69|||||||||
79741|Wade Amphibolite|71862|2|Defined|p6-p7, p10, p15, p22|Statherian|Statherian|Named for the Wade Dam on Uno Station and is exposed in the northeastern Eyre Peninsula as isolated outcrops and subcrops on Cooyerdooo, Shirrocoe, Gilles Downs and Corunna stations. The type locality is a small hill 2.1km south of Lake Gilles Paddock on the northern shore of Lake Gilles, Corunna Station, Eyre peninsula comprising tht eare extending 100m radially from the point 675808mE, 6384534mN, GDA94, Zone 53. This unit is intersected in drillholes DDH LED001 (drillhole 229988) and RDD002 (drillhole 229989). Geochemistry is discussed. Ages are derived from Reid and Jagodzinski, 2011. See also p28-p30, p36, p41-p42, p45, p53, p57-p58.|1736 +/- 4 Ma and 1737 +/- 5 Ma|Moola Suite||Intruded by the Deuter Diorite. Intrudes the Sleaford Complex and (inferred) the Cooyerdoo Granite.|Fine- to coarse-grained amphibolite composed of hornblende, clinopyroxene, plagioclase, biotite, K-feldspar and quartz.|20-APR-23
24068|Waganny Dacite|24346|5|Briefly described|p98 Fig.1|||Of Gawler Range Volcanics.||||||
24068|Waganny Dacite|40430|2|Defined|p7|Mesoproterozoic|Mesoproterozoic|||||||
24068|Waganny Dacite|41619|6|Mentioned|Map legend|Mesoproterozoic||||||||
24068|Waganny Dacite|41972|5|Briefly described|p370, p378-381, p384|||||||||03-AUG-09
24068|Waganny Dacite|42466|5|Briefly described|Map Legend|||||||||
24068|Waganny Dacite|42475|4|Described|p15|||part of "older" Gawler Range Volcanics||||||
24068|Waganny Dacite|42546|5|Briefly described|Map legend|Mesoproterozoic||||||||
24068|Waganny Dacite|42736|5|Briefly described|map legend|Mesoproterozoic||||||||
24068|Waganny Dacite|43052|5|Briefly described|p109|||of Gawler Range Volcanics||||||
24068|Waganny Dacite|50605|5|Briefly described|p(ii), 8.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Gawler Craton & Curnamona Province. Of the Lower Gawler Range Volcanics. Age: 1591 +/- 3Ma (U-Pb).||||||
24068|Waganny Dacite|65221|5|Briefly described|p28 Fig.3a |Mesoproterozoic|Mesoproterozoic|Of Gawler Range Volcanics||||||
24068|Waganny Dacite|65922|6|Mentioned|p16, p17 Tb.2|Calymmian|Calymmian|Unit in lower sequence of Gawler Range Volcanics. Type area 1.5 km WSW of Waganny Dam; 150 m thick. Reddish-brown porphyritic dacite grading to rhyodacite. Is conformably overlain by Bittali Rhyolite. 1591 +/- 3 Ma U-Pb zircon (Fanning et al. 1988).||||||20-MAR-15
24068|Waganny Dacite|67900|6|Mentioned|p20-21|Mesoproterozoic|Mesoproterozoic||1591 +/- 3 Ma (Fanning et al., 1988).|Lower Gawler Range Volcanics.||||
24068|Waganny Dacite|68126|5|Briefly described|p21||||1591 +/- 3 Ma (U-Pb zircon: Fanning et al., 1986).|Basal Gawler Range Volcanics.||||
24068|Waganny Dacite|68158|5|Briefly described|p4|||||Gawler Range Volcanics.|||Porphyritic reddish-brown dacite to rhyodacite, includes dark green-grey dacite and andesite.|
24068|Waganny Dacite|69649|5|Briefly described|p34|||[Misspelt as Wanganny].|1591 +/- 3 Ma; U-Pb zircon (Fanning et al., 1988).|Unit in Gawler Range Volcanics.||||26-FEB-15
24068|Waganny Dacite|70659|5|Briefly described|p5-8|Mesoproterozoic|Mesoproterozoic|SW and S margins of the Gawler Ranges.||Lower Gawler Range Volcanics.||Overlain by Bittali Rhyolite.|Porphyritic rhyodacitic to dacitic autobrecciated lavas interlayered with crystal-rich volcaniclastic facies, intruded by polymict volcanic breccia dykes.|
24068|Waganny Dacite|70816|5|Briefly described|p4-5,198|||SW and S Gawler Ranges margin.||Unit of lower Gawler Range Volcanics.||Overlain by Bittali Rhyolite. Underlain by an unnamed succession of quartz-phyric rhyolite.|Rhyodacitic to dacitic sequence of lavas and crystal-rich volcaniclastics|
24068|Waganny Dacite|71317|5|Briefly described|p25, p96, p176|||Part of a single eruptive sequence.||||Overlain by the Bittali Rhyolite.||
24068|Waganny Dacite|71418|6|Mentioned|p21|Mesoproterozoic|Mesoproterozoic|Geological province: Gawler Craton.||||||
24068|Waganny Dacite|72065|5|Briefly described|p105|Calymmian|Calymmian|Geological province: Gawler Craton.||Unit of Gawler Range Volcanics.||||
24068|Waganny Dacite|72090|4|Described|p11-p12, p15, p60-p62, p64-p65|||Gawler Craton. Intersected by MSDP08 drillhole.||Gawler Range Volcanics, Lower||Unconformably overlies the Sleaford Complex, Peter Pan Supersuite.|Moderate reddish brown, porphyritic, fine- to medium-grained dacite; minor poorly sorted, medium- to coarse-grained volcaniclastic intervals.|
24068|Waganny Dacite|72459|6|Mentioned|p46|||||||||
24068|Waganny Dacite|72464|6|Mentioned|p2|Mesoproterozoic|Mesoproterozoic|Gawler Craton.||||||
24068|Waganny Dacite|73104|6|Mentioned|p3, p41, p46|Mesoproterozoic|Mesoproterozoic|Intercepted in drillhole MSDP09 and MSDP08.||||Underlain by Sleaford Complex.|Includes dacitic lavas and volcaniclastics.|
24068|Waganny Dacite|73110|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|This age is of an equivalent at Toondulya Bluff.|1591 +/- 3 Ma (U-Pb).|Lower Gawler Range Volcanics.|||Dacite-rhyodacite, porphyritic; dacite; andesite.|
29929|Waitoona beds|23288|6|Mentioned|Fig.5||Early Ordovician|||||||
29929|Waitoona beds|43052|5|Briefly described|Fig. 2.10|||||||||
29929|Waitoona beds|43053|5|Briefly described|Map Legend|Devonian|Ordovician|Alluvial fan sandstone and conglomerate.||||||25-MAY-05
29929|Waitoona beds|43258|5|Briefly described|Map Legend|Devonian|Ordovician|||||||
29929|Waitoona beds|43298|5|Briefly described|Map Legend|Devonian|Ordovician|||||||
29929|Waitoona beds|60953|5|Briefly described|Map Legend|Permian|Carboniferous|Alluvial fan sandstone and conglomerate. Geological Province: Officer Basin.||||||
29929|Waitoona beds|61108|5|Briefly described|map legend|Permian|Permian|Alluvial fan sandstone and conglomerate. Geological Province: Officer Basin.||||||02-JUN-05
29929|Waitoona beds|65376|6|Mentioned|p9 Fig.1.2. |Paleozoic|Paleozoic||||||Alluvial fan sediments.|
29929|Waitoona beds|68131|5|Briefly described|p2 Fig.1|Permian|Permian|Alluvial fan deposits.||||||
24069|Walkandi Formation|13497|5|Briefly described|p64, p104, p112|Triassic|Triassic|Simpson Basin. ||||Equivalent to the Nappamerri Formation and Tinchoo Formation.||
24069|Walkandi Formation|22839|6|Mentioned|P33|||Lateral equivalent of the Tinchoo Formation||||||
24069|Walkandi Formation|22883|5|Briefly described|P29, Fig2||Triassic|Overlain by Peera Peera Formation.||||||14-DEC-06
24069|Walkandi Formation|24204|5|Briefly described|p262, 270, 263 Fig.4|Triassic|Triassic|Probable equivalent to Nappamerri Group (Cooper Basin). Overlain by Peera Peera Formation (unconformable). Geological Province: Simpson Basin.||||||
24069|Walkandi Formation|41063|2|Defined|p40|Middle Triassic|Early Triassic|Previously named "Unnamed redbeds" E - M.||||||14-DEC-06
24069|Walkandi Formation|41176|6|Mentioned|Fig.3|||||||||
24069|Walkandi Formation|41183|6|Mentioned|p308|||See also Fig.3||||||
24069|Walkandi Formation|41536|5|Briefly described|p384|||||||||
24069|Walkandi Formation|42008|4|Described|p266|||||||||
24069|Walkandi Formation|42463|6|Mentioned|Fig.4 P171|||||||||
24069|Walkandi Formation|42746|4|Described|p6, Fig.2 p4|||||||||
24069|Walkandi Formation|43052|5|Briefly described|Table 2.1|||||||||
24069|Walkandi Formation|44133|5|Briefly described|p43, 94|Triassic|Triassic|Conformably underlies: Peera Peera Formation. Thickness: 134m.||||||
24069|Walkandi Formation|62376|5|Briefly described|p84|Middle Triassic|Late Permian|Geological Province: Pedirka Basin.||||||09-FEB-10
24069|Walkandi Formation|64778|6|Mentioned|p13|Triassic|Triassic|Simpson Desert Basin.||||||
24069|Walkandi Formation|65238|5|Briefly described|p7 Fig. 8, p9, p14 Fig. 17|Early Triassic|Early Triassic|Unconformable below Peera Peera Fm. In:Simpson Desert Basin.Shallow/ephemeral/lacustrine deposits of basal red beds, grading up into a slightly carbonaceous shale/siltstone succession in basinal areas. Lithology: interbedded shale/siltstone/minor sst||||||
24069|Walkandi Formation|65489|5|Briefly described|p55, p58, p61-63, p137, p149, p151|Middle Triassic|Early Triassic|Simpson Basin. Restricted in area to the Poolowanna Trough depocentre. Shallow ephemeral lacustrine environment. 130m thick. Tight, potential seal to underlying Permian where present. Possible local reservoir development.||||Is overlain conformably by Peera Peera Formation. Correlated with Tinchoo Formation; probably equivalent to Arrabury Formation.|Interbedded shale, siltstone and minor sandstone redbeds; with low porosity and permeability.|
24069|Walkandi Formation|69454|5|Briefly described|p38:3-4, 6, 7 Fig.38.6; 38:8-9, 13|Anisian|Changhsingian|Moore (1986). Pedirka Basin (subsurface only). 247m thick in Blamore-1. Shallow ephemeral lacustrine deposits (continental red-beds). Forms an important regional seal.||||Unconformably overlies Purni Formation. Underlies Poolowanna Formation unconformably, and by Peera Peera Formation disconformably or unconformably. Correlated with Arrabury Formation (Cooper Basin).|Interbedded shale, siltstone and minor very fine to fine sandstone. All have a distinctive colour ranging from grey-green/maroon to brick red.|12-JUL-16
24069|Walkandi Formation|69457|6|Mentioned|p41:5 Fig.41.4|||||||||12-JUL-16
24069|Walkandi Formation|69673|5|Briefly described|p149, p151, p152, p154 fig 126, p161|Triassic|Triassic|Maximum thickness of 247m.||||Unconformably overlies Purni Formation, unconformably overlain by Poolowanna Formation|Interbedded shale, siltstone and minor very fine grained to fine grained sandstone.|
24069|Walkandi Formation|69946|4|Described|p8, p36, p51-52|Early Triassic|Early Triassic|Poolowanna Trough, Simpson Basin. Of Moore (1986). Type section is the interval 2768 - 2902m in Poolowanna 1. Up to 134m thick.||||Is overlain conformably by Peera Peera Formation. Correlated with Arrabury Formation (Cooper Basin).|Oxidised, pale grey, grey-green, brick-red, brown and maroon shale and siltstone interbedded with minor pale grey-green, very fine- to fine-grained sandstone.|
24069|Walkandi Formation|69948|6|Mentioned|Fig.4.18|||Eromanga Basin.||||Unconformably overlies Purni Formation. Is overlain by Peera Peera Formation.||
24069|Walkandi Formation|71321|6|Mentioned|p15|||Of Simpson Basin.||||Overlain by the Peera Peera Formation.||24-OCT-19
24069|Walkandi Formation|71342|4|Described|Ch4 p25, Ch5 p8-p9|Early Triassic|Early Triassic|Poolowanna Trough, Simpson Basin. Originally identified as unnamed redbeds by Weiltshire (1978) before being defined by Moore (1986). A type section in Poolowanna 1 is mentioned. A maximum thickness of 134m is recorded in Poolowanna 2. Age derived from palynofloras. See also Ch5 p30, Ch5 p36, Ch5 p51-p52, Ch9 p18, Ch12 p3, Ch12 tbl 12.1, Ch12 p12.||||Conformably overlain by the Peera Peera Formation. Equivalent to the Arrabury Formation of the Cooper Basin.|Oxidised, pale grey, grey-green, brick-red, brown or maroon shale and siltstone interbedded with minor pale grey-green, very fine to fine-grained sandstone.|
24069|Walkandi Formation|72476|6|Mentioned|p36 Fig.9|||Simpson Basin. Time-temperature thermal history diagram.||||||
24069|Walkandi Formation|73281|6|Mentioned|p1, Appendix (DIP)|||[Misspelt as Walikandi Formation, p1]. Pedirka Basin. See DIP034_Petroleumdata.xlsx and DIP034_Welldata.xlsx. Also written as Walkandi Formation, lower and Walkandi Formation, upper.||||||
23126|Wallaroo Group|22629|5|Briefly described|p152|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
23126|Wallaroo Group|23491|6|Mentioned|p18|||Correlatives with phyllites in Sthn Eyre Peninsula.||||||
23126|Wallaroo Group|23719|5|Briefly described|p16 Table 3|Paleoproterozoic|Paleoproterozoic|Geological Province: Gawler Craton.||||||07-NOV-08
23126|Wallaroo Group|23803|5|Briefly described|p28|Paleoproterozoic|Paleoproterozoic|Age: 1770-1730Ma. Geological Province: Gawler Craton.||||||07-NOV-08
23126|Wallaroo Group|24360|6|Mentioned|p53|||Geological Province: Yorke Peninsula, Gawler Craton||||||
23126|Wallaroo Group|24475|2|Defined|p48|Paleoproterozoic|Paleoproterozoic|Intruded by Tickera and Arthurton Granites. Not related to Wallaroo Basalt (QLD).||||||04-AUG-09
23126|Wallaroo Group|24507|6|Mentioned|p25|||Includes Wandearah Formation.||||||
23126|Wallaroo Group|24585|5|Briefly described|p32|Statherian|Statherian|Contains a succession of metasediments and metavolcanic rocks in the northern area - which host the Moonta-Wallaroo cooper deposits. Age: 1770-1740Ma. Intruded by Tickera Granite, Curramulka Gabbronorite and Arthurton Granite.||||||23-DEC-09
23126|Wallaroo Group|43561|6|Mentioned|p1438|||||||||
23126|Wallaroo Group|50081|6|Mentioned|p43|Statherian|Statherian|Age: ~1750 Ma.||||||
23126|Wallaroo Group|50605|5|Briefly described|p8.6, 8.7|||Intruded by Hiltaba Supersuite. Geological Province: Gawler Craton and Curnamona Province.||||||18-JAN-07
23126|Wallaroo Group|60953|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Chemical and clastic metasediments and metavolcanics. Age: 1763-1738Ma.||||||07-NOV-08
23126|Wallaroo Group|60958|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Low-grade metasediments and metavolcanics in the eastern Gawler Craton. Age: ~1770-1740Ma. Geological Province: Gawler Craton.||||||09-JUL-13
23126|Wallaroo Group|61108|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|Chemical and clastic metasediment and felsic to mafic metavolcanic rock. Age: 1763-1738 Ma.||||||07-NOV-08
23126|Wallaroo Group|61121|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Comprises Wandearah, Weetulta and Matta Formations. Low-grade (greenschist to lower amphibolite facies) metasediments and metavolcanics in the eastern Gawler Craton. Geological Province: Gawler Craton.||||||09-JUL-13
23126|Wallaroo Group|61262|5|Briefly described|p455 Fig. 11|Paleoproterozoic|Paleoproterozoic|Age: >1750Ma. Geological Province: eastern Gawler Craton.||||||07-NOV-08
23126|Wallaroo Group|62592|5|Briefly described|p73.|Paleoproterozoic|Paleoproterozoic|Eastern Gawler Craton. A volcano-sedimentary succession similar to the Willyama Supergroup.|1760 Ma.|||||
23126|Wallaroo Group|62729|5|Briefly described|p39 Fig. 1b, p40|Paleoproterozoic|Paleoproterozoic|Metasedimentary and metavolcanic rocks including MOONTA PORPHYRY. Age: <1850 to ~1740 Ma. Comprises upper thin bedded argillite and carbonate-bearing strata, and lower meta-arkosic (qtz - K-feldspar - muscovite) rocks. Geological Province: Gawler Craton.||||||07-NOV-08
23126|Wallaroo Group|63020|5|Briefly described|p987 Fig. 8|Paleoproterozoic|Paleoproterozoic|Geological Province: Gawler Craton (Olympic Domain).||||||07-NOV-08
23126|Wallaroo Group|63223|6|Mentioned|p17 Fig. 2, p19|||Adjacent to the Curnamona Province.||||||30-APR-07
23126|Wallaroo Group|63224|6|Mentioned|p7|||||||||
23126|Wallaroo Group|63275|6|Mentioned|p14 Fig.1.|Paleoproterozoic|Paleoproterozoic|||||||
23126|Wallaroo Group|63398|5|Briefly described|p661, p663|Paleoproterozoic|Paleoproterozoic|Age: 1770-1740Ma. Metasediments and metavolcanics. Intruded by Hiltaba Suite granitoids including Tickera Granite and Arthurton Granite. On the Yorke Peninsula. ||||||07-NOV-08
23126|Wallaroo Group|63866|4|Described|p6, p9, p21, p30|Statherian|Statherian|Olympic Domain, Gawler Craton. Hosts IOCG deposits of the Moonta-Wallaroo area on Yorke Peninsula. Contain detrital zircons of c. 1850 ma age presumably sourced from Donington Suite granitoids or volcanic equivalents.|c. 1740 Ma||Includes the Moonta Porphyry|||
23126|Wallaroo Group|64130|5|Briefly described|p1378 Fig.1, p1380 Fig.2, p1381, p1387  |Paleoproterozoic|Paleoproterozoic|Eastern Gawler Craton. Deformed c.1577 Ma (synchronous with emplacement of Tickera Granite).|1760-1740 Ma (Cowley et al., 2003).|||||
23126|Wallaroo Group|64131|5|Briefly described|p1399 Fig.2, p1400-1402, p1405-1409   |Paleoproterozoic|Paleoproterozoic|Deformed during 1.73 to 1.71 Ga Kimban orogeny. Petrophysical properties.|ca 1.76 to 1.74 Ga (Cowley et al., 2003)||||Metasedimentary and bimodal volcanic rocks metamorphosed to greenschist or amphibolite facies. The sedimentary rocks are metapelites to fine-grained psammites, with interlayered BIF and calc-silicate horizons.|
23126|Wallaroo Group|64132|5|Briefly described|p1415, pp1417-1421, pp1432-1435.   |Paleoproterozoic|Paleoproterozoic|Comprises large areas of basement in the Olympic Dam district. |c.1760 - 1740 Ma (Jagodzinski 2005).|||Is overlain unconformably by Pandurra Formation.|Thin-bedded feldspathic to biotite-rich metasiltstones, metacarbonate rocks, minor banded iron formation, and rare carbonaceous metapelitic rocks.|
23126|Wallaroo Group|64133|4|Described|p1443-1445, p1447-1448 Tb.1 |Paleoproterozoic|Paleoproterozoic|See also p1449-1453, p1460 Tb.5, p1462-1464. Eastern margin, Gawler Craton. Important host sequence for several IOCG alteration sequences.|~1765-1740 Ma||Includes Moonta Porphyry.||Upper part comprises thin-bedded feldspathic to biotite-rich or carbonaceous metasiltstones, metacarbonate rocks, felsic and mafic-volcanics rocks, and minor BIF.|
23126|Wallaroo Group|64233|5|Briefly described|p25|Paleoproterozoic|Paleoproterozoic|Age: ~1790-1750Ma. In the Olympic Domain on NW corner of Yorke Peninsula. Shows evidence of deformation at the greenschist to lower amphibolite-grade.||||||07-NOV-08
23126|Wallaroo Group|64313|5|Briefly described|p450 Fig. 1|Paleoproterozoic|Paleoproterozoic|Geological province: Gawler Craton.||||||09-FEB-10
23126|Wallaroo Group|64725|6|Mentioned|p58 Fig.2. |||Gawler Craton.||||||
23126|Wallaroo Group|64726|6|Mentioned|p83 Fig.2.|||||||||
23126|Wallaroo Group|64741|5|Briefly described|p299 Fig. 2|Paleoproterozoic|Paleoproterozoic|Age: 1770-1750Ma. Geological province: Gawler Craton.||||||07-FEB-11
23126|Wallaroo Group|64744|6|Mentioned|p367.|Statherian|Statherian||1765-1735 Ma.|||||
23126|Wallaroo Group|65219|6|Mentioned|p27|Paleoproterzoic|Paleoproterzoic|1850-1740 Ma, deposition age of Wallaroo Group and other units.||||||22-SEP-09
23126|Wallaroo Group|65221|5|Briefly described|p26|Palaeoproterozoic|Palaeoproterozoic|1745Ma, Cleve Domain. Intruded by Gawler Range Volcanics and Hiltaba Suite.||||||10-MAR-10
23126|Wallaroo Group|65375|4|Described|pp7-8, pp12-13, pp19-23, p46.|Paleoproterozoic|Paleoproterozoic|Dominates basement in northern Yorke Peninsula. A succession of metasediments, felsic and mafic volcanics, deformed by Kimban Orogeny 1730-1700 Ma and later intruded. Host to Moonta and Wallaroo copper mines.|c.1770-1740 Ma.||Includes Wandearah, Weetulta and Matta Formations.|Probably overlies Gleesons Landing Granite. Intruded by Tickera Granite, Curramulka Gabbronorite and Arthurton Granite. Unconformably overlain by Rhynie Sandstone.|Bimodal volcanics and metasediments: mainly siliciclastics with minor carbonate or carbonate-siliciclastics-mixed facies in eastern part.|
23126|Wallaroo Group|65376|4|Described|p9 Fig.1.2, pp101-111.|Paleoproterozoic|Paleoproterozoic|High-grade metamorphism and complex deformation from 1730-1700 Ma Kimban Orogeny. |c.1763-1741 Ma.|||Includes Wandearah, Weetulta and Matta Formations. Intruded by Hiltaba Suite granites.|Chemical and clastic metasediments, and felsic and mafic volcanic rocks.|
23126|Wallaroo Group|65390|4|Described|p18|Statherian|Statherian|Gawler Craton. Comprises all meta-sedimentary and meta-igneous units older than Tickera-Arthurton Granites and the Oorlana Metasomatite within the Moonta Domain (Conor, 1995).  Includes Wardang Volcanics, Willamulka Volcanics, Wanderah Metasiltstone, Doora Metasediments. 1760 +/- 7 Ma age from interbedded Moonta Volcanics (U-Pb zircon; Fanning, pers. comm., 2002).||||||10-JAN-14
23126|Wallaroo Group|65485|6|Mentioned|p42, Fig 1|Paleoproterozoic|Paleoproterozoic|Easternmost Gawler Craton. May correlate with Price Metasediments.||||Overlies the Sleaford Complex.|Volcaniclastics and sediments.|09-JUL-13
23126|Wallaroo Group|65915|5|Briefly described|p3 Fig.2, p5, p18-19|Statherian|Statherian|Sedimentary and volcanic rocks deposited between c.1790-1740 Ma east of Kalinjala Mylonite Zone. Intruded by Hiltaba Suite. ~1760-1720 Ma. A metasiltstone sample contains detrital zircon dated at ~3300 Ma, similar to detrital zircons in Cooyerdoo Granite.||||||
23126|Wallaroo Group|65922|6|Mentioned|p29 Fig.6|||Shown on Fig.6 as c.1750 Ma.||||||
23126|Wallaroo Group|66302|4|Described|p6, p18, p29-30, p33-34, p47, p63-65|Paleoproterozoic|Paleoproterozoic|Olympic Domain, Gawler Craton. Deposited in a fluvial-aeolian to shallow-water and shelfal marine settings, probably in a back-arc tectonic setting. See also p75-77, p88.|ca. 1760 - 1740 Ma (Cowley et al, 2003)||Includes the Wandearah Metasiltstone, Weetulta Formation and the Matta Formation.|Equivalent to the Moonabie Formation. Intruded by the Tickera, Arthurton and Roxby Downs Granites.|Metasedimentary rocks and mafic and felsic metavolcanic rocks.|
23126|Wallaroo Group|66916|6|Mentioned|p9, p14|Paleoproterozoic|Paleoproterozoic|Yorke Peninsula.|c.1760 Ma.|||||
23126|Wallaroo Group|67058|5|Briefly described|p476, p490, p494 Fig.14.|Paleoproterozoic|Paleoproterozoic|Mount Woods Domain and Fowler Domain, northern Gawler Craton. Contains detrital zircon populations with age peaks of c.2520-2500, 2000, 1850-1840 and 1790-1720 Ma.|c.1760 - c.1740 Ma (Fanning et al. 2007).||Includes Wandearah Formation.|||
23126|Wallaroo Group|67181|5|Briefly described|p629|Statherian|Statherian|Gawler Craton. Fanning et al. 2007|||Includes Weetulta Formation|||
23126|Wallaroo Group|67323|5|Briefly described|Eastern Australia Time-Space Plot; p32|||Gawler Craton.|1752 +/- 8 Ma.|||||
23126|Wallaroo Group|67536|5|Briefly described|Map Legend|Statherian|Statherian|Gawler Craton.|ca. 1765 +/- 27 Ma - 1741 +/- 7 Ma||Includes Weetulta Formation and Wandearah Formation.||Undifferentiated metasediments and felsic and mafic metavolcanic rocks.|
23126|Wallaroo Group|67581|6|Mentioned|p45|||Gawler Craton. Pre-Kimban (1790-1740 Ma) Orogeny.||||||
23126|Wallaroo Group|67870|5|Briefly described|p11, p15-16|||Folded and metamorphosed. Forms a seismic zone of low reflectivity, about 9km thick.||||Is overlain unconformably by Gawler Range Volcanics.||
23126|Wallaroo Group|67900|6|Mentioned|p20, 22|Paleoproterozoic|Paleoproterozoic|Cowley et al. (2003). Eastern Gawler Craton. Deformed during the c.1577 Ma Kararan Orogeny.|c.1760 Ma.|||||
23126|Wallaroo Group|67980|6|Mentioned|p550|Paleoproterozoic|Paleoproterozoic|||||||
23126|Wallaroo Group|68131|5|Briefly described|p2 Fig.1|Paleoproterozoic|Paleoproterozoic||||||Included in a polygon of chemical and clastic metasediments and felsic and mafic volcanic rocks.|
23126|Wallaroo Group|68158|5|Briefly described|p1-2, p5, p16-17|||Yorke Peninsula. Includes some volcanic units.|~1750 Ma.||Wandearah Metasiltstone.|||
23126|Wallaroo Group|69048|6|Mentioned|p3|||Eyre Peninsula / Yorke Peninsula.|c.1775-1750 Ma.|||||
23126|Wallaroo Group|69554|6|Mentioned|p128|||Fanning et al. (2007). Gawler Craton.|c.1760 Ma.||||Volcano-sedimentary sequence.|
23126|Wallaroo Group|69591|6|Mentioned|p106 Fig.2.100|||Appears in a diagram of the geodynamic setting of ~1760-1740 Ma eastern Australia.||||||
23126|Wallaroo Group|69666|6|Mentioned|p27 Fig.3|Paleoproterozoic|Paleoproterozoic|||||||
23126|Wallaroo Group|69748|5|Briefly described|p179-181, 198|Paleoproterozoic|Paleoproterozoic|Moonta-Wallaroo region, Olympic IOGC Province. Affected by the Kimban Orogeny.|1760-1740 Ma.||Wandearah, Weetulta Formations.||A diverse suite of siltstone-dominated metasedimentary, felsic and mafic volcanic rock packages.|
23126|Wallaroo Group|70027|5|Briefly described|p56-57,72|Statherian|Statherian|Geological province: Gawler Craton. Deposited at ca. 1763-1741 Ma just prior to the 1730-1690 Ma Kimban Orogeny. Coeval with Warramboo magnetite gneiss, Moonabie Formation, Price Metasediments.|ca. 1763-1741 Ma|||||
23126|Wallaroo Group|70286|6|Mentioned|p892|||Southern Gawler Craton.|||||Siliciclastic sediments. Intercalated with felsic and mafic volcanic rocks aged c.1750 to 1740 Ma.|
23126|Wallaroo Group|70334|5|Briefly described|p10,75|Statherian|Statherian|Geological province: Gawler Craton. Of Yorke Peninsula, Moonta region. Deformed by the ~1590-1555 Ma Kararan Orogeny. Synchronous with emplacement of Tickera Granite.|1760-1745 Ma|||Equivalent to Moonabie Formation.||
23126|Wallaroo Group|70382|5|Briefly described|p27, p32, p35|Statherian|Statherian|Geological province: eastern Gawler Craton. Possible source for some of Quartoo Sand Member inherited zircon.|~1750 - ~1740 Ma|||Underlain by Donington Suite, and intruded by granites and gabbros of Hiltaba Suite||
23126|Wallaroo Group|70383|6|Mentioned|p51|Statherian|Statherian|Mentioned as a possible source of zircons aged c.1732 +/- 20 Ma, extracted from the Sprigg Diamictite Member.||||||
23126|Wallaroo Group|70405|6|Mentioned|p12 figure 4|Paleoproterozoic|Paleoproterozoic||1750 Ma|||||
23126|Wallaroo Group|70511|6|Mentioned|p86-87, 98|Paleoproterozoic|Paleoproterozoic|Gawler Craton.||||Surrounds (?is intruded by) Roxby Downs Granite.||
23126|Wallaroo Group|70659|5|Briefly described|p4|Palaeoproterozoic|Palaeoproterozoic|Deformation synchronous with intrusion (i.e. c.1575 Ma).||||Intruded by Tickera Granite.||
23126|Wallaroo Group|70893|6|Mentioned|p3 fig 1a|Statherian|Statherian||c. 1760 Ma|||||
23126|Wallaroo Group|70947|5|Briefly described|p960, 961|Statherian|Statherian|Geological province: Gawler Craton. Metasediments and volcanics intruded by Hiltaba Suite granites.|ca. 1750 Ma|||Intruded by Hiltaba Suite granites.|Metasediments and volcanics.|
23126|Wallaroo Group|71037|6|Mentioned|p20, p21 Fig.1|Paleoproterozoic|Paleoproterozoic|Developed as part of a large, lithologically complex shallow marine basin that includes the Wallaroo Group.||||Shown as younger than McGregor Volcanics and Moonabie Formation and older than Peter Pan Supersuite.||
23126|Wallaroo Group|71043|5|Briefly described|p104, p107-108|Statherian|Statherian|Gawler Craton. Had granite basement thrust over it during the Kararan Orogeny.|c.1750 Ma (maximum depositional age).||||Widespread arenaceous and lesser carbonaceous sedimentary rocks, and associated mafic and felsic volcanics.|
23126|Wallaroo Group|71129|5|Briefly described|p14,17-18,35,37,39,203|Statherian|Statherian|Geological Province: Olympic Domain, Gawler Craton. Deposited in a rift continental shelf setting. Basement to Moonabie and Wandearah formations.|c. 1760-1740 Ma||Includes Wandearah Formation.|Overlain by Moonabie or Pandurra Formations. Underlain by Corny Point Paragneiss and Donington Suite. Temporally equivalent to Moonabie Formation.||
23126|Wallaroo Group|71317|5|Briefly described|p15-p16|Palaeoproterozoic|Palaeoproterozoic|Olympic Domain, Gawler Craton.|1760-1740 Ma|||||
23126|Wallaroo Group|71322|5|Briefly described|p100|||Southern Gawler Craton.|c.1750-1740 Ma.||||Felsic and mafic volcanic rocks intercalated with siliciclastic sediments.|
23126|Wallaroo Group|71341|6|Mentioned|p179 fig 1, p188 fig 7, p194, p196|Palaeoproterozoic|Palaeoproterozoic|Broadly geochemically similar to the Moonabie Formation, Price Metasediments, Cleve Group, McGregor Volcanics .|ca. 1765-1740 Ma|||||
23126|Wallaroo Group|71348|6|Mentioned|p201|Statherian|Statherian|Geological province: Gawler Craton.||||||
23126|Wallaroo Group|71534|6|Mentioned|p295-296,301|Statherian|Statherian|Geological province: Gawler Craton.|c. 1750 Ma|||||
23126|Wallaroo Group|71536|5|Briefly described|p1, p99, p107, p114|Statherian|Statherian|Ages are SHRIMP U-Pb dates and are interpreted as the age of magmatic crystallisation. Petrography, zircon characteristics and geochronology results are discussed for two granite samples of this suite.|1748 +/- 12 Ma |||||
23126|Wallaroo Group|71559|6|Mentioned|p15 Fig 1|Paleoproterozoic|Paleoproterozoic|Geological province: Gawler Craton.||||||
23126|Wallaroo Group|71712|6|Mentioned|p410 Fig 1, p423|Paleoproterozoic|Paleoproterozoic|Metamorphosed during 1730-1690 Ma Kimban Orogeny.|1750 Ma||Includes Wandearah Formation.||Siliceous, carbonaceous and calc-silicate metasediments and felsic to mafic volcanics.|
23126|Wallaroo Group|71799|4|Described|p150 fig 2, p165|Statherian|Statherian|Eastern Gawler Craton.|ca 1875 Ma||Includes the  Moonta Formation, Mona Formation and the Matta Formation.|Overlies the Myola Volcanics.|Silicic volcanics, porphyry, basalt, dolerite and siltstone, carbonaceous shale and dolomite.|03-OCT-18
23126|Wallaroo Group|71859|5|Briefly described|p3-p4, p6|Paleoproterozoic|Paleoproterozoic|Olympic Domain, southern Gawler Craton.|1760-1740 Ma|||||
23126|Wallaroo Group|71862|6|Mentioned|p3, p21|||||||||
23126|Wallaroo Group|71895|4|Described|p2, p10-p12, p27, p33, p47, |Paleoproterozoic|Paleoproterozoic|Punt Hill region. Alteration and mineralisation are discussed. Spectral analysis, protolith interpretation, mineralogy and 3D geological models are discussed. See also p49-p50, p54-pp55, p57, p61-p63, p83, p89-p92, p106, p116-p117, p134-p135, p142-p148, p152, p154, APP4. p4-p7.|||Includes the Wandearah Formation.|Overlies the Donington Suite. Overlain by the Gawler Range Volcanics.|Sedimentary rocks.|
23126|Wallaroo Group|72090|6|Mentioned|p8, p10|Statherian|Orosirian|Olympic Domain, Gawler Craton.|c. 1760-1740 Ma|||||
23126|Wallaroo Group|72462|6|Mentioned|p3, p10|Paleoproterozoic|Paleoproterozoic|Gawler Craton, Olympic Domain.||||Equivalent to Moonabie Formation.|Unmetamorphosed sediments.|
23126|Wallaroo Group|72463|6|Mentioned|p2|Paleoproterozoic|Paleoproterozoic|||||||
23126|Wallaroo Group|72488|5|Briefly described|p2 Fig.1, p4|||Eastern Gawler Craton. Forms part of the basement to the Olympic Dam District.|1.76 - 1.74 Ga.|||Is intruded by the Hiltaba Suite. Is overlain unconformably by the Gawler Range Volcanics.|(Meta)sedimentary rocks.|
23126|Wallaroo Group|72949|6|Mentioned|p34|Statherian|Statherian||ca. 1.75 Ga|||||
23126|Wallaroo Group|73026|5|Briefly described|p6-7, p9-11|Paleoproterozoic|Paleoproterozoic|Northern Yorke Peninsula.|c. 1750 Ma||Includes the Wardang Volcanics. Moonta Porphyry, Mona Volcanics.|Overlies the Myola Volcanics and the Broadview Schist.|Schist; argillite; rhyolite, porphyritic, fine grained; limestone; siltstone.|
23126|Wallaroo Group|73027|5|Briefly described|p6-p7, p9-11|Statherian|Statherian|Eastern Eyre Peninsula/Yorke Peninsula. Includes Greenschist facies fabrics.|c. 1750 Ma||Includes the Wardang Volcanics, Moonta Porphyry, Mona Volcanics.||Volcanic rocks and interlayered sediments including Schist, argillite, rhyolite, porphyritic, fine grained; limestone; siltstone.|
23126|Wallaroo Group|73030|5|Briefly described|p2147-2154|Statherian|Statherian|Gawler Craton, Olympic Cu-Au Province. The presence of widespread scapolite-albite alteration within with these lithologies is taken as evidence that evaporites were part of the stratigraphy.|ca. 1790 to 1740 Ma||||Siltstone, sandstone, and carbonate sedimentary rocks.|
23126|Wallaroo Group|73092|6|Mentioned|p1-2, p19, p23, p26, p41-43, p49|Statherian|Statherian|Yorke Peninsula region. Geophysical data indicate this unit is intruded by a large, shallow crustal granitic body.|c. 1770 Ma||Wardang Volcanics Member, Renowden Metabasalt Member||Metasedimentary and meta-igneous rocks.|
23126|Wallaroo Group|73103|5|Briefly described|Map legend.|||Is shown in the Solid Geology Interpretation map, below the main Whyalla 250k map.||||||
23126|Wallaroo Group|73110|5|Briefly described|Map legend.|||Shown in the Solid Geology Interpretation map below the main PORT AUGUSTA map.||||||
23126|Wallaroo Group|73130|6|Mentioned|[poster] Fig. 1|Paleoproterozoic|Paleoproterozoic|||||||28-OCT-22
23126|Wallaroo Group|73155|6|Mentioned|p264 Fig.1, p280-281|Statherian|Statherian|Gawler Craton.|ca. 1750 Ma||Mona Volcanics Member, Wardang Volcanics Member|||
23126|Wallaroo Group|73162|6|Mentioned|p449, Fig.1|Statherian|Statherian||1760-1740 Ma|||||
23126|Wallaroo Group|73165|5|Briefly described|p619-621, 624, 635-636, 638|Paleoproterozoic|Paleoproterozoic|Gawler Craton, Moonta Domain, Olympic Domain. Deformation, metamorphism and metasomatism at ca 1600-1575 Ma synchronous with emplacement of Tickera Granite. Upper greenschist facies in the northern Yorke Peninsula, amphibolite facies in the southern Yorke Peninsula.  Two phases of deformation locally preserved at Wallaroo North Beach, isoclinal folds from the first phase were refolded in the later phase by open upright folds, Type 3 fold interference pattern. Also occurs as metasedimentary xenoliths in Tickera Granite.|ca 1750 Ma||Wandearah Formation, Matta Formation|Intruded by Tickera Granite and Arthurton Granite.|Metasediments and metavolcanics. Upper greenschist to amphibolite facies.|
23126|Wallaroo Group|73166|6|Mentioned|p644, 645, Fig. 1|Paleoproterozoic|Paleoproterozoic|Gawler Craton, eastern. 1.76 Ga age shown in Fig. 1, p645.|ca 1.75 Ga||||Volcanic and metasedimentary formations.|
23126|Wallaroo Group|73235|6|Mentioned|p52-53, p63|Statherian|Statherian|Gawler Craton. Olympic and Spencer regions. Hosts Moola and Olympic Dam IOCG mineralisation. Hosts gold mineralisation in the Olympic mineral field of the Kararan (Hiltaba Suite) gold mineral system.|c. 1750 Ma|||||
23126|Wallaroo Group|73298|6|Mentioned|p1073|Statherian|Statherian|Gawler Craton.|1760-1740 Ma|||||
23126|Wallaroo Group|73302|6|Mentioned|p33||||c.1750 Ma.|||||
23126|Wallaroo Group|73493|5|Briefly described|p712, p714 Fig.1, p716 Fig.3, p722, p727|Statherian|Statherian|Gawler Craton.|ca 1765-1735 Ma||Wardang Volcanics, Renowden Metabasalt Member|Overlies Donington Suite|Metasedimentary and metavolcanic succession, includes metabasic units.|
23126|Wallaroo Group|73525|5|Briefly described|p19 Fig.13, p20|Statherian|Statherian|Olympic Domain.|1772+/-14 Ma, 1735+/-10 Ma||||Clastics, felsic extrusives, carbonates, siliciclastics, mafic extrusives.|
23126|Wallaroo Group|73644|5|Briefly described|p1-3, p7 Fig.4, p12-15|Paleoproterozoic|Paleoproterozoic|Upper greenschist to amphibolite facies in the Yorke Peninsula.|1770-1740 Ma|||Intruded by Hiltaba Suite|Dominated by metamorphosed fine-grained psammites, siltstones, calc-silicates, albitites, quartzites and iron-rich sediments.|
23126|Wallaroo Group|74361|6|Mentioned|p163, 173|Paleoproterozoic|Paleoproterozoic|Eastern margin of Gawler Craton. Deformed by the Kimban Orogeny (~1730-1690 Ma).|1760-1740 Ma.||||Metasediments.|
34770|Wallatinna Member|22922|6|Mentioned|33 fig 2|||||||||
34770|Wallatinna Member|23282|2|Defined|p74||Early Cambrian|Age: Early Cambrian 524 - 522Ma. of Officer Basin. Defined by Benbow (1982) as Wallatinna Formation. redefined as a member of Observatory Hill Formation as not easily distinguished from conglomerate facies of Cadney Park Member.||||||
34770|Wallatinna Member|24112|5|Briefly described|p254 Fig.2|Early Cambrian|Early Cambrian|Of the Marla Group. Geological Province: Officer Basin||||||
34770|Wallatinna Member|62570|5|Briefly described|p580 Figs. 2 and 3|Middle Cambrian|Middle Cambrian|Of Observatory Hill Formation (Marla Group). Geological Province: Officer Basin.||||||10-AUG-07
34770|Wallatinna Member|72478|6|Mentioned|p8|Early Cambrian|Early Cambrian|Officer Basin. Shown as Wallatinna Formation Fig.7 p70.||Observatory Hill Formation||||29-MAR-21
68095|Walparuta Formation|60485|6|Mentioned|p28, p29|||Andalusite-bearing graphitic pelite.||||||
68095|Walparuta Formation|61736|5|Briefly described|p666 Fig. 3|Paleoproterozoic|Paleoproterozoic|Of Saltbush Subgroup (Strathearn Group) Geological province: Olary Domain.||||||
68095|Walparuta Formation|62535|5|Briefly described|p666 Fig.3, p672|Paleoproterozoic|Paleoproterozoic|Olary Domain.|c.1690 Ma.|Saltbush Subgroup.||||
68095|Walparuta Formation|62993|6|Mentioned|p2, p3, p6, p37|Paleoproterozoic|Paleoproterozoic|Olary Domain.||Saltbush Group||Overlies Plumbago Formation and Raven Hill Subgroup, overlain by Strathearn Group.||16-DEC-21
68095|Walparuta Formation|63102|4|Described|p14,32-35|||Geological province: Olary Domain, Curnamona Province. Occurs in the Weekeroo and Ameroo Hill Areas. Underlain by a sequence of thin graphitic pelite, which is equivalent to Plumbago Formation.||Unit of Saltbush Subgroup.||Underlain by Plumbago Formation. Equivalent to Sundown Group, possibly Broken Hill Group.|Bedded pelite to psammopelite with variable distribution of generally thin psammite layers.|22-OCT-19
68095|Walparuta Formation|63866|5|Briefly described|p41|||||||Equivalent to the Sundown Group. Overlain by the Strathearn Group.|Pelite and psammopelite with minor psammite layers and rare calc-silicate nodules.|
68095|Walparuta Formation|64741|5|Briefly described|p301 Fig. 4|Paleoproterozoic|Paleoproterozoic|Of Saltbush Group. Geological province: Olary Domain. Equivalent in Broken Hill Domain is Sundown Group.||||||07-FEB-11
68095|Walparuta Formation|64742|6|Mentioned|p321 Fig.3, P323.|||||Unit in Saltbush Subgroup.|||Quartz-mica schist.|29-MAR-12
68095|Walparuta Formation|64944|5|Briefly described|p28 Fig. 1, p29 Tb. 1|Paleoproterozoic|Paleoproterozoic|Of Saltbush Group. Geological province: Olary Domain. Pelite and psammopelite with minor psammite layers. Equivalent to ?Sundown Group units in Broken Hill Domain.||||||07-FEB-11
68095|Walparuta Formation|66302|5|Briefly described|p36 Fig.9, p38, p39|Statherian|Statherian|Olary Domain, Curnamona Province. ||Saltbush Group|||Metamorphosed mudstone and siltstone with minor sandstone layers and rare calc-silicate nodules.|
68095|Walparuta Formation|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Olary Domain.||Saltbush Group.||||
68095|Walparuta Formation|70405|4|Described|p9 table 1, p29, p41, p96|Paleoproterozoic|Paleoproterozoic|Correlation remains uncertain, is similar to the Black Maria Formation and the Sundown Group.|1670 Ma|Saltbush Group||Overlies Plumbago Formation, correlated with Sundown Group|Pelite dominated with interbedded thin psammite layers; basal fine grained graphitic schist.|
68095|Walparuta Formation|70657|4|Described|p14-15, p17, p20, p33-34, p40-42, p44|Statherian|Statherian|Curnamona Province; Olary Domain. Formerly the Walparuta Schist. May be equivalent to Sundown Group of Broken Hill Domain.|<1693 Ma - >1655 Ma|Saltbush Group||Underlies Alconie Formation (Strathearn Group). Overlies Plumbago Formation and ?Oonartra Creek Formation (Raven Hill Subgroup). May be equivalent to Sundown Group of Broken Hill Domain.|Interlayered pelite, psammopelite, and thinly bedded psammite. Some beds are graded; local calcsilicate ellipsoids. Distinctly graphitic base. Fibrolite, andalusite and tourmaline are locally common.|
68095|Walparuta Formation|70658|5|Briefly described|p2, 7, 10, 15, 19, 25, 29|Paleoproterozoic|Paleoproterozoic|Walparuta Inlier, Olary Domain, Curnamona Province.|~1680 Ma.|Saltbush Group.||Locally overlies Plumbago Formation. Equivalent to Sundown Group.|Interbedded psammopelite, pelite and garnetiferous psammite.|
68095|Walparuta Formation|73429|5|Briefly described|p106 Fig.2, p107|Statherian|Statherian|Curnamona Province, Olary Domain.||Saltbush Group||Overlies Raven Hill Subgroup, underlies Mount Howden Subgroup||
39163|Wandearah Formation|24475|2|Defined|p50|Paleoproterozoic|Paleoproterozoic|Of Wallaroo Group.  Formerly referred to as Wandearah Metasiltstone and Wandearah Metasediments.||||||07-NOV-08
39163|Wandearah Formation|24507|6|Mentioned|p25|||Of the Wallaroo Group. Carbonaceous metasiltstone.||||||
39163|Wandearah Formation|60958|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Wallaroo Group. Metasandstone, argillite, siltstone, carbonate, calcsilicate and occasional conglomerate. Geological Province: Gawler Craton.||||||07-NOV-08
39163|Wandearah Formation|61121|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|All metasediments in the Wallaroo Group on Yorke Penisula, including metasandstone, argillite, siltstone, carbonate, calcsilicate and occasional conglomerate. Geological Province: Gawler Craton.||||||07-NOV-08
39163|Wandearah Formation|63398|5|Briefly described|p666, p671 Fig. 7|||Contains the Aagot Member and Doora Member. See also p671 Fig. 7.||||||
39163|Wandearah Formation|65375|5|Briefly described|p19.|Paleoproterozoic|Paleoproterozoic|Includes all late Paleoproterozoic metasediments on Yorke Peninsula.||Unit in Wallaroo Group.|Comprises Aagot, Doora, New Cornwall, Wokuma and Ninnes Members.|||
39163|Wandearah Formation|65376|5|Briefly described|p101. |||||Unit in Wallaroo Group.|Includes Doora, Aagot, Delken, New Cornwall and Wokurna Members.|||
39163|Wandearah Formation|66302|5|Briefly described|p29, p30, p33|||Olympic Domain, Gawler Craton. Also referred to as the now obsolete Wandearah Metasiltstone on p29. ||Wallaroo Group||Equivalent to the Moonabie Formation.|Metasedimentary rocks including a metasiltstone.|
39163|Wandearah Formation|67058|5|Briefly described|p496.|||Contains c.1750 Ma zircons with eHf values between -5 and 0 (Belousova et al. 2006, 2009).||Unit in Wallaroo Group.||||
39163|Wandearah Formation|67181|5|Briefly described|p634, p635 Fig.17|Statherian|Statherian|Gawler Craton|ca 1750 Ma (Belousova et al. 2006, 2009)||||Metasediments|
39163|Wandearah Formation|67536|6|Mentioned|Map Legend|Statherian|Statherian|Gawler Craton.|ca. 1765 +/- 27 Ma - 1741 +/- 7 Ma|Of the Wallaroo Group.|||Chemical and clastic metasediments.|
39163|Wandearah Formation|68208|6|Mentioned|p37 Fig.8|||||||||
39163|Wandearah Formation|69748|5|Briefly described|p179-181, 183|Paleoproterozoic|Paleoproterozoic|Moonta-Wallaroo region, Olympic IOGC Province. First appears as Wanderah Formation on p179; again on p181.||Wallaroo Group.|Doora, New Cornwall Members.||Metasediments (chloritic schists) and a range of banded feldspar and calc-silicates and carbonate-rich units.|
39163|Wandearah Formation|70659|4|Described|p9-11, p13-14, p36, p40, p44, p58-60|Palaeoproterozoic|Palaeoproterozoic|See also p78-114, p286-288, p301-302, p320, p324, p327-341, p360-361, p363-367. Part of basement to the Olympic Domain. Separated from Moonabie Formation by Angle Dam Fault. Graphic core logs. Thin section descriptions.||||Overlain unconformably by Fresh Well Formation, Roopena Basalt. Thrust over Moonabie Formation.|Purple-red massive calcareous mudstone and siltstone with minor fine grained sandstone, dolomite and greywacke beds.|
39163|Wandearah Formation|70721|6|Mentioned|p64|Paleoproterozoic|Paleoproterozoic|||||||
39163|Wandearah Formation|70816|6|Mentioned|p3|Paleoproterozoic|Paleoproterozoic|Gawler Ranges region.||||||
39163|Wandearah Formation|70948|6|Mentioned|p974|Paleoproterozoic|Paleoproterozoic|Geological province: Gawler Craton.||||||
39163|Wandearah Formation|71037|5|Briefly described|p22-23 Fig.2, p27 Fig.6|Paleoproterozoic|Paleoproterozoic|Shown  on the Six Mile Hill 1:75,000 surface geology map (p22-23 Fig.2) and Interpreted bedrock geology (p27 Fig.6).||||Shown as younger than Moonabie Formation and  older than Wortham Granite, Moonabie Suite.|Massive to laminated dolomitic micaceous siltstone and fine-grained micaceous sandstone with lesser dolomite and greywacke.|
39163|Wandearah Formation|71129|4|Described|p1,35,37-39,69,73,75,104-105|Statherian|Statherian|Geological Province: Olympic Domain, Gawler Craton. Informally named as Mount Laura Formation (SAMEDAN Oil Corporation of Australia, 1985). Preserved in a narrow NS-trending graben bounded by Roopena and Randell faults to the west (juxtaposed against Braodview Schist), and Angle Dam Fault to the east (juxtaposed against Moonabie Formation). Exposures are dominated by low broad rises of in situ pebble to cobble lag to subcrop. Intersected in numerous drillholes : SAMEDAN SOC 5, SAMEDAN SOC 8, SAMEDAN SOC 9 and ESSO ROP 6. Thrust over the Moonabie Formation via the Angle Dam Fault (N-S striking reverse fault, W-dipping; SAMEDAN 1985). Contains quartz-tourmaline veins and breccias associated with the Roopena Fault system. Contains thin basal conglomerate with pebbles similar in appearance to Moonabie Formation. Typically moderately weathered, affected by mottled white bleaching, and often indurated by calcrete or silicified. Deposition was synchronous with A-type felsic and mafic magmatism of the Weetulta and Matta formations (Zang 2006). Older zircon age spectra indicate a Gawler Craton detrital source (Jagodzinski, 2005); feldspar and detrital muscovite indicate a granitic source. Lithology is discussed in some detail. See also p142,177,184,187-188,201,203-205,225,227.|1762+\-7 Ma (MDA, Jagodzinki, 2005)|Unit of Wallaroo Group.||Overlain by Angle Dam Volcanics or Roopena Basalt. Intruded by Gairdner Dolerite. Equivalent in part to the Wallaroo Group. Faulted against the Broadview Schist.|Massive to laminated dolomitic micaceous meta-siltstone and fine-grained micaceous meta-sandstone, with minor dolomite and conglomeratic greywacke beds.|13-NOV-19
39163|Wandearah Formation|71130|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic||||||Massive to laminated, dolomitic micaceous siltstone and fine-grained micaceous sandstone with lesser dolomite and greywacke.|
39163|Wandearah Formation|71131|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic||||||Massive to laminated, dolomitic micaceous siltstone and fine-grained micaceous sandstone with lesser dolomite and greywacke.|
39163|Wandearah Formation|71235|6|Mentioned|p5, p8|Palaeoproterozoic|Palaeoproterozoic|||||||
39163|Wandearah Formation|71348|6|Mentioned|p208,214-215|||Geological province: Aileron Province, Arunta Region. See p215 for summary of U-Pb geochronological data. Deposited after 1760 Ma.|< 1760 Ma.|||||
39163|Wandearah Formation|71413|5|Briefly described|p32, 33, 37, 38|Statherian|Statherian|Geological province: Gawler Craton.  Show metasomatic alteration near contact with Samphire granite.|1763-1750 Ma|||Intruded by Samphire granite.||
39163|Wandearah Formation|71414|6|Mentioned|p42 Fig 1|Paleoproterozoic|Paleoproterozoic|Geological province: Gawler Craton.||||||
39163|Wandearah Formation|71712|6|Mentioned|p423, 424|||||Of Wallaroo Group|||Includes chloritic and carbonaceous metasediments.|
39163|Wandearah Formation|71895|4|Described|p2, p10, p27, p33, p36, p38|||Equivalents of this unit unconformably overlie the Donington Suite basement. Spectral analysis and mineralogy are discussed. This unit is interpreted to be associated with a moderate density anomaly above background values. This unit is associated with Cu-Au prospects where skarns have developed. See also p47, p106, p125, p141, p147, p154, APP1. p6-p20, APP4. p4, APP5. p20, p47, p49, p51,  p53, p55, p57, p65, p67-p68, p70-p71, p73, p75, p77, p92, p94-p95, p97, p99, p101, p103, p117,  p119, p121, p123, p125, p129, p131, p133, p135, p137, p139,  p145, p147, p149, p151, p153, p155, p157, p166, p168, p170, p172. APP6 p174-p178, p187, p189, APP8. p201-p202  . Petrographic description for numerous samples provided. Intersected in drillholes OCDD01, GHDD01, GHDD06,WDDD01, WPDD01, PDDD01 and HODD03.||Wallaroo Group|||Laminated, silty feldspathic metasedimentary rocks including conglomerates, breccias, sandstones and siltstones. Skarns also present.|
39163|Wandearah Formation|72089|6|Mentioned|p3|Palaeoproterozoic|Palaeoproterozoic|Gawler Craton.||||||
39163|Wandearah Formation|72090|6|Mentioned|p14|||Gawler Craton.||||||
39163|Wandearah Formation|72237|6|Mentioned|p29|Paleoproterozoic|Paleoproterozoic|Geological province: Gawler Craton.||||||
39163|Wandearah Formation|73026|5|Briefly described|p9|Paleoproterozoic|Paleoproterozoic||||||Argillite; quartz siltstone; carbonate, calcsilicate, iron-rich, carbonaceous; metasandstone.|
39163|Wandearah Formation|73027|5|Briefly described|p9,|Palaeoproterozoic|Palaeoproterozoic||||||Argillite, quartz siltstone, carbonate, calcsilicate, iron-rich, carbonaceous; metasandstone.|
39163|Wandearah Formation|73092|6|Mentioned|p2|Paleoproterozoic|Paleoproterozoic|||||||
39163|Wandearah Formation|73103|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Is also shown in the Solid Geology Interpretation map, below the main Whyalla 250k map.|||||Argillite, muscovite; quartz siltstone; metasediments, alkali feldspar, carbonate, calc-silicate, iron-rich, carbonaceous; metasandstone.|
39163|Wandearah Formation|73110|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic||||||Argillite, muscovite; quartz siltstone; metasediments, alkali feldspar, carbonate, calc-silicate, iron-rich, carbonaceous; metasandstone. Red-brown medium-coarse poorly-sorted thin-bedded sandstone (mapped separately).|
39163|Wandearah Formation|73162|6|Mentioned|p448, p450-453|Paleoproterozoic|Paleoproterozoic|||||Onlapped unconformably by Gawler Range Volcanics. Underlies Fresh Well Formation.|Includes siltstone, sandstone.|
39163|Wandearah Formation|73165|5|Briefly described|p621, 623|Paleoproterozoic|Paleoproterozoic|Gawler Craton, Moonta Domain, northern Yorke Peninsula. Dominates the Wallaroo Group.||Wallaroo Group||Interlayered with Weetula Formation.|Metasediments including fine-grained psammites, siltstones, calc-silicates, albitites, quartzites and iron-rich sediments.|
39168|Wandilta Amphibolite Member|24475|2|Defined|p55|Paleoproterozoic|Paleoproterozoic|Of Matta Formation.||||||07-NOV-08
39168|Wandilta Amphibolite Member|65376|6|Mentioned|p101 Fig.3.1.|||||||||
24076|Wangary Gneiss|22629|6|Mentioned|p148|Siderian|Siderian|Age: 2479+/-8Ma.||||||02-JUN-09
24076|Wangary Gneiss|23791|6|Mentioned|p2|Archean|Archean|Part of the Sleaford Complex.  Age: 2479 +/- 8Ma.  Geological Province: Gawler Craton.||||||02-JUN-09
24076|Wangary Gneiss|24526|6|Mentioned|p98|||See also p96 Fig. 2 - mentioned only in the context of its precursor during 2800-2600Ma.||||||
24076|Wangary Gneiss|40448|5|Briefly described|p27|||||||||
24076|Wangary Gneiss|40644|6|Mentioned|p120, p124 Fig. 3|||Also referred to as Wangary Gneisses (Fanning in Parker et al 1981). Included in the Sleaford Complex. Intruded by Kiana Granite. Geological province: Gawler Craton. Age information in Fig. 4.||||||13-AUG-08
24076|Wangary Gneiss|43052|4|Described|p38,Table 3.1|||Of Sleaford Complex.||||||27-MAY-08
24076|Wangary Gneiss|50605|5|Briefly described|p4.2, 8.7|||Geological Province: Gawler Craton and Curnamona Province. Of the Dutton Suite (Sleaford Complex).||||||02-JUN-09
24076|Wangary Gneiss|61070|5|Briefly described|Map Legend|Proterozoic|Archean|Of the Sleaford Complex. Massive to compositionally layered feldspar-quartz-biotite-muscovite gneiss.  Intruded by Kiana Granite. Metamorphic age: 2479 +/- 9Ma (U-Pb Zircon). Geological Province: Gawler Craton.||||||12-JAN-10
24076|Wangary Gneiss|61307|5|Briefly described|p35|Archean|Archean|Part of the Sleaford Complex. Age: 2497+/-8Ma. Geological Province: Gawler Craton.||||||07-NOV-08
24076|Wangary Gneiss|63866|5|Briefly described|p18|Siderian|Siderian|Coulta Domain, Gawler Craton. |c. 2485 Ma|||||
24076|Wangary Gneiss|64131|5|Briefly described|p1401|||||Of the Sleaford Complex|||Amphibolite facies paragneiss.|
24076|Wangary Gneiss|64828|5|Briefly described|p1065 Fig. 2, p1067|Late Archean|Late Archean|Included in the Sleaford Complex. Amphibolite facies. See also the misspelt Wangary Gneisses.||||||04-MAR-09
24076|Wangary Gneiss|65376|5|Briefly described|p15, pp33-35. |||Inherited or protolith igneous zircons crystallised at c.2485 Ma and c.2685 Ma.|2462 +/- 11 Ma.|||Intruded by Dutton Suite.|Amphibolite facies, grey, garnetiferous, layered quartzofeldspathic gneisses; characteristically biotite-rich.|
24076|Wangary Gneiss|65485|6|Mentioned|p42|Archean|Archean|Amphibolite facies unit of the Sleaford Complex.||||||
24076|Wangary Gneiss|66302|5|Briefly described|p10, p11, p13, p14, p61, p61 Fig.14|Neoarchean|Neoarchean|Protolith interpreted to have been deposited between 2535 and 2500 Ma in an extensional back arc setting. SHRIMP age interpreted as maximum crystallization age of the igneous protolith of this unit.|2679 +/- 9 Ma (SHRIMP U-Pb, Fanning, 1997)|Sleaford Complex|||Amphibolite facies, K-feldspar-plagioclase gneisses.|
24076|Wangary Gneiss|66882|6|Mentioned|p116|Siderian|Siderian|Contains inherited c.2700 Ma zircons from the southern Gawler Craton basement.|2460 Ma|||||
24076|Wangary Gneiss|67536|5|Briefly described|Map Legend||Neoarchean|Gawler Craton. ?igneous protolith 2679 +/- 9 Ma.|2679 +/- 9 Ma|Of the Sleaford Complex.|||Igneous protolith?|
24076|Wangary Gneiss|67721|6|Mentioned|p36|Siderian|Siderian||c. 2460 Ma|||||
24076|Wangary Gneiss|68131|6|Mentioned|p66|Paleoproterozoic|Archean|Coffin Bay Peninsula.||||||
24076|Wangary Gneiss|68208|6|Mentioned|p31 Fig.2||Paleoproterozoic|Minimum detrital zircon age ~2480 Ma.||Of Sleaford Complex||||
24076|Wangary Gneiss|71235|6|Mentioned|p14||||2520-2500 Ma (Fanning et al., 2007)|||||
24076|Wangary Gneiss|71859|4|Described|p2, p6-p9, p14, p28, p36|||Southern Gawler Craton. Exposed in the Southwest of Point Sir Isaac on Coffin Bay Peninsula.||Sleaford Complex||Intruded by Kiana Granite|Massive to layered, K-feldspar-plagioclase-quartz-biotite-muscovite-andalusite gneiss.|11-APR-23
24076|Wangary Gneiss|73256|6|Mentioned|p559|||||Sleaford Complex|||Medium- to high-grade metamorphics.|
73298|Wangerrip Supersequence|63134|2|Defined|110-111|||||||||
73298|Wangerrip Supersequence|63269|5|Briefly described|p605|Eocene|Late Cretaceous|Otway Basin.||||Overlies Sherbrook Supersequence. Is overlain by Nirranda Supersequence.||
73298|Wangerrip Supersequence|69297|6|Mentioned|p79, p80, p110, p115|||||||||
73298|Wangerrip Supersequence|69651|5|Briefly described|p6,p10, p12-15, p17-23, p28, p33, p39-40|Eocene|Late Cretaceous|See also p42-47, p49-50. Maastrichtian to early Eocene age. Forms the base of the Australia-Antarctica post-breakup succession. Shallow-marine, marginal marine and deltaic deposits. Generally less than 500m thick; locally up to 1,534m. Modelling diagrams.||||Overlies Sherbrook Supersequence. Is overlain by Nirranda Supersequence.|Sandstone and siltstone.|17-JUN-20
73298|Wangerrip Supersequence|70077|6|Mentioned|Regional: p4-5|Cenozoic|Cenozoic|Otway Basin.||||||
73298|Wangerrip Supersequence|70078|5|Briefly described|Regional: Fig.4; p3-4|Eocene|Paleocene|Sandstones of this unit are likely reservoirs in the Sorell Basin.||||Overlies Sherbrook Supersequence. Is overlain by Nirranda Supersequence.||
73298|Wangerrip Supersequence|70880|6|Mentioned|p77|Eocene|Paleocene|Otway Basin. Post-rift sedimentation; coastal plain, deltaic and inner-shelf settings.||||Overlies Sherbrook Supersequence. Is overlain by Nirranda Supersequence.||
73298|Wangerrip Supersequence|71266|5|Briefly described|p614 Fig.3, p615|Eocene|Paleocene|Otway Basin. Latest Maastrichtian to midddle Eocene.||||Overlies Sherbrook Supersequence. Is overlain by Nirranda Supersequence.||
33834|Wanna Megacrystic Granite Gneiss|22489|5|Briefly described|p13|Proterozoic|Proterozoic|||||||
33834|Wanna Megacrystic Granite Gneiss|61070|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Donington Suite. Weakly to strongly foliated, coarse-grained megacrystic granite-granodiorite to augen gniess. Characteristic ovoid zoned plagioclase and K-feldspar megacrysts up to 40mm wide. Geological Province: Gawler Craton.||||||12-JAN-10
33834|Wanna Megacrystic Granite Gneiss|65375|6|Mentioned|p16.|||Eyre Peninsula. Suggested correlative with the augen orthogneiss phase of Gleesons Landing Granite.||||||
33834|Wanna Megacrystic Granite Gneiss|68131|5|Briefly described|p6, p13, p42-43, p47-48, p52|Paleoproterozoic|Paleoproterozoic|Schwarz (2003). Eyre Peninsula. Metamorphosed and migmatised at 1713 +/- 5 Ma (zircon rims). Is eqiuvalent to dated samples of the Gleesons Landing Granite and  to Augen Orthogneiss described by Zang (2002)|c.1850 Ma.|Donington Suite.|||Includes late-stage mylonite zones with syn-kinematic leucosomes and pegmatites.|02-MAR-20
33834|Wanna Megacrystic Granite Gneiss|73122|6|Mentioned|p34|||||||Is intruded by deformed dykes of Tournefort Metadolerite.||
33834|Wanna Megacrystic Granite Gneiss|73634|5|Briefly described|p5, 8-9, 11|||Wilson et al. (2020). Wanna, Jussieu Peninsula. Microstructure discussed in detail.||||Is intruded by Tournefort Metadolerite dykes.|Coarse-grained granite with signs of plastic deformation; moderately strained; cut by boudinaged dykes.|
82230|Wanna Megacrystic Orthogneiss|73027|5|Briefly described|p25-28|Orosirian|Orosirian|Wanna is the type locality of this unit. Geochronology is discussed in detail.|1847 +/- 4 Ma (Reid et al, 2007)|Donington Suite|||leucocratic coarse-grained metagranitoid consisting of megacrystic K-feldspar augen, quartz, plagioclase, biotite and hornblende.|05-AUG-21
24560|Waraco Limestone|23314|5|Briefly described|331 Fig.2|||||||||
24560|Waraco Limestone|37854|6|Mentioned|Table 1|||||||||
24560|Waraco Limestone|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Willouran||||||
24560|Waraco Limestone|39348|6|Mentioned|Map legend|Adelaidean|Adelaidean|Willouran||||||
24560|Waraco Limestone|40225|4|Described|Map sheet|||||||||
24560|Waraco Limestone|40294|3|Fully described|p24|||See also P63||||||
24560|Waraco Limestone|41403|5|Briefly described|p67|||||||||
24560|Waraco Limestone|42222|6|Mentioned|Table 1 P5|||||||||
24560|Waraco Limestone|42882|5|Briefly described|Fig.2, P4|||of Callanna Group||||||
24560|Waraco Limestone|43052|5|Briefly described|p175,Table 6.1|||of Curdimurka Subgroup.||||||
24560|Waraco Limestone|60959|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Of the Curdimurka Subgroup.  Pale grey to cream stromatolitic dolomite and calcitic and dolomitic marble; limestone, stromatolites.||||||
24560|Waraco Limestone|64793|6|Mentioned|p285 fig 4|||Adelaide Rift Complex.||Unit in Callanna Group.||||
24560|Waraco Limestone|72492|6|Mentioned|p2 Fig.1, p2|Neoproterozoic|Neoproterozoic|In the Worumba Anticline.||Curdimurka Subgroup||Overlies Kirwan Siltsone and underlies Worumba Dolomite.||
24560|Waraco Limestone|73222|5|Briefly described|p6-7|Tonian|Tonian|Flinders Ranges. Torrensian. One of few carbonate units within the Callanna Group. Slightly older than Dunns Mine Limestone.||Curdimurka Subgroup, Callanna Group, Warrina Supergroup||Underlain by Kirwan Siltstone. Overlain by Worumba Dolomite. Possibly equivalent to Boorloo Siltstone.|Pale grey to cream stromatolitic dolostone and calcitic to dolomitic marble.|
73257|Warakurna Supersuite|63864|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Includes Giles Suite.||||||
73257|Warakurna Supersuite|64408|5|Briefly described|map legend|Mesoproterozoic|Mesoproterozoic|Date shown: 1050-1178 Ma, (S. S. Sun 1996), for Giles Complex. Subdivided into 3 unnamed and one informally named unit.||||||16-SEP-08
73257|Warakurna Supersuite|64580|6|Mentioned|map legend|||||||||
73257|Warakurna Supersuite|65135|5|Briefly described|p1, p6 Fig.4, p12 Fig.8, p13-14, p16||Stenian|Groups all igneous rocks related to the ~1075 Ma Giles Event. Minimum age of ~1078 Ma. Contains Skirmish Hill Volcanics. Crops out over ~1.5 million sq km of central and western Australia, forming the Warakurna Large Igneous Province. In the western Musgrave Complex, largely occurs within and to the SW of the Tjuni Purlka Tectonic Zone||||||
73257|Warakurna Supersuite|65506|5|Briefly described|p986, p987 Fig. 1A||c.1070 Ma.|Also known as Warakurna Large Igneous Province. Overlies the Collier Group. Sills form part of Bangemall Supergroup.||||||
73257|Warakurna Supersuite|65693|5|Briefly described|p1, p3, p5, pp8-15.|Mesoproterozoic|Mesoproterozoic|The magmatic expression of the Giles Event: mafic and felsic intrusions outcropping over 1.5 million km2 of central and western Australia; took place over c.60 m.y. Hosts Ni-Cu-PGE mineralization.|c.1078 - c.1067 Ma.||Includes Skirmish Hill Volcanics and Alcurra Suite, as well as un-named layered intrusions and massive gabbro.|||
73257|Warakurna Supersuite|65833|5|Briefly described|p1, p6-7 Figs.4-5, p12 Fig.8, p13-16|Stenian|Stenian|Groups all igneous rocks related to the ~1075 Ma Giles Event. Includes layered mafic-ultramafic intrusions, unlayered gabbro and comagmatic leucogranite, and possible remnants of bimodal volcanics. Magmatism may have occurred as punctuated events over 60 m.y. Crops out across ~1.5 million sq. km in central and western Australia. A-type character. Includes Skirmish Hill Volcanics.||||||
73257|Warakurna Supersuite|65898|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Includes Giles Suite mafics and ultramafics (>1078 Ma) and 9 ungrouped unnamed granitic units (1075-1060 Ma).||||||
73257|Warakurna Supersuite|65899|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Age shown as c.1070 Ma. Includes Glenayle and Prenti Dolerites.||||||
73257|Warakurna Supersuite|65906|5|Briefly described|p3-4|||Gabbros, granites and mafic dykes. West Musgrave Block. Contains all igneous rocks related to the c.1080 Ma Giles Event: Bentley Supergroup and Giles Complex.||||||
73257|Warakurna Supersuite|65907|6|Mentioned|p6.|||Interpreted as a mantle plume event.||||||
73257|Warakurna Supersuite|66104|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Shown as consisting of Kulkatharra Dolerite sills which intrude into the Edmund and Collier Groups. Age shown as c.1070 Ma.||||||
73257|Warakurna Supersuite|66256|5|Briefly described|p4 Fig.3, p11 Fig.8, p16, see comments|Stenian|Stenian|In west Musgrave Province. Intruded mainly along tectonic margins of Tjuni Purlka Tectonic Zone. In Musgrave Province, incorporates Giles intrusions (giant layered mafic-ultramafic intrusions). Age: 1073, 1074 and 1075 Ma, SHRIMP, Whole rock Nd isotopic data, 6 analyses (GSWA and GA). Geochron (SHRIMP) results for crystallization age: Mamutjarra Zone 1026+/-26 to 1078+/-3 Ma; Tjuni Purlka Tectonic Zone 1052+/-11 to 1078+/-5 Ma. Sources: GSWA and GA. See also p18 Fig.14, p29 Fig.26, p31-32, p41, p53-54 App.1, 57-59 App.3, p71 App.4.|||||Includes locally rapakivi-textured, syenogranites, quartz syenites, and monzogranites.|11-JAN-17
73257|Warakurna Supersuite|66280|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Age shown as >1078-1060 Ma. Includes Giles Suite and several unnamed units: mylonitic syenogranite and leucogranite; fine-grained leucocratic syenogranite; porphyritic to seriate syenogranite; and massive biotite syenogranite. ||||||
73257|Warakurna Supersuite|66281|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic||||Includes Giles Suite and un-named units of olivine gabbro, syenogranite and monzodiorite.||Mafic intrusive rocks and layered mafic-ultramafic intrusives.|
73257|Warakurna Supersuite|66282|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|In this map area, is shown as consisting of Giles Suite rocks aged >1078 Ma as well as four separately-mapped but un-named more felsic intrusive units aged 1075 - 1060 Ma..|>1078 - 1060 Ma.||Includes Giles Suite.||Intrusive mafic and ultramafic rocks, variably metamorphosed; minor felsic intrusives: syenogranite, granodiorite, monzogranite.|
73257|Warakurna Supersuite|66284|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Apart from Giles Suite, includes a syenogranite with mafic xenoliths.|||Includes Giles Suite and an un-named but separately-mapped syenogranite unit.|||
73257|Warakurna Supersuite|67128|4|Described|p5 Fig.3, p6-7, p10-11|||All magmatic rocks formed during the Giles Event in the western Musgrave Province. Voluminous mafic and A-type felsic intrusions. Thought to have formed during the Warakurna LIP magmatism.|>1078 to c.1026 Ma.||Giles intrusions, Alcurra Dolerite.|Intrudes the Tollu Group.|Layered mafic-ultramafic intrusions, massive gabbros, mafic dykes, and rare granitic rocks.|
73257|Warakurna Supersuite|67136|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Warakurna Large Igneous Province.|c.1070 Ma.||Includes Kulkatharra Dolerite.|Intrudes Edmund and Collier Groups.||
73257|Warakurna Supersuite|67244|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Also contains five separately-mapped but un-named sub-units.|1078 - 1074 Ma.||Includes Giles Suite and Alcurra Dolerite.|||
73257|Warakurna Supersuite|67372|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Map includes 17 separate, un-named units. Ultramafic intrusives and granites.|1078 - 1060 Ma.||Includes Giles Suite, Alcurra Dolerite, and 17 un-named units.||Layered mafic-ultramafic intrusions; dolerite dykes, sills and plugs; granitic intrusions.|
73257|Warakurna Supersuite|67375|3|Fully described|p5, p13, pp33-38, pp216-230, pp340-347.|Mesoproterozoic|Mesoproterozoic|Groups all igneous intrusive and extrusive rocks related to the 1085-1040 Ma Giles Event. Outcropping across 1.5 million km2 of central and western Australia, it forms the Warakurna Large Igneous Province. Mafic to felsic magmatism; granites have a strong A-type geochemical signature. Hosts economically significant mineral deposits.|1078 +/- 3 - 1062 +/- 10 Ma.||Includes Bentley Supergroup, Giles Suite and Alcurra Dolerite.|Intrudes Wankanki Supersuite.|Giant layered mafic-ultramafic 'Giles intrusions', massive gabbros mixed amd mingled with granite, dolerite, granite plutons, and mafic and felsic lavas.|10-NOV-15
73257|Warakurna Supersuite|67553|4|Described|p2,7-8,11-12,15-17,20,27,31,34-35|Stenian|Stenian|Geological province: Musgrave Province, North Australian Craton. Mafic and felsic intrusions into rocks of the Musgrave Province during 1085-1040 Ma Giles Event. Outcrops across ~1.5 million km2 of central and western Australia, forming the Warakurna LIP (Wingate et al., 2004; Morris and Pirajno, 2005). Volcanic components of the Warakurna Supersuite are also grouped as part of the Bentley Supergroup. Associated with the Ngaanyatjarra Rift, a long-lived intracontinental rift setting. Locally strongly deformed during the Petermann Orogeny (coinciding with global Pan-African period of plate reorganisation during Gondwanan assembly). Deposition occuring at ?1085-?1040 Ma (GSWA data). See also p38,58,73,95.|c. 1085-1040||Includes Alcurra Dolerite, Giles intrusions and Kunmarnara Group.|||
73257|Warakurna Supersuite|68077|5|Briefly described|p3 Fig.1, p5-6, p11, p19-23, p31-38|Mesoproterozoic|Mesoproterozoic|Emplaced during the 1085-1040 Ma Giles Event; over at least 1.5 million km2 to form the Warakurna Large Igneous Province. Isotopic composition (Lu-Hf and Sm-Nd) and evolution tabulated and discussed in detail.|1075-1067  Ma (U-Pb zircon)||||Dolerite, basalt, komatiite, gabbro, granophyre, basaltic andesite, gabbronorite, troctolite, norite, olivine and biotite gabbros.|07-SEP-17
73257|Warakurna Supersuite|68100|5|Briefly described|p2, 5, 7, 15, 26, 28, 32, 33|Mesoproterozoic|Mesoproterozoic|Includes giant layered-mafic intrusions (Giles intrusions), mafic dykes, and granites.|1075-1060 Ma|||Intrudes/overlies Kunmarnara Group|Layered mafic intrusions, mafic dykes and granites. Locally rapakivi textured granites. Includes charnokitic syenogranite.|19-JAN-17
73257|Warakurna Supersuite|68186|5|Briefly described|p30|Mesoproterozoic|Mesoproterozoic|Wingate et al. (2004). Widespread unit.|c.1075 Ma.|||||
73257|Warakurna Supersuite|68561|6|Mentioned|500K_GEOLOGYP08_LUT.csv||Mesoproterozoic|||||||23-OCT-15
73257|Warakurna Supersuite|68995|5|Briefly described|p1-2, p5, p22, p28-33, p43, p46 Fig.22|Stenian|Stenian|Volcanic rocks are the dominant lithology of the Bentley Basin. Geochemistry briefly discussed. See also p48 Fig.24, p54 Fig.29, p57 Fig.31, p59, p66, p74.|c. 1080 - 1045 Ma (SHRIMP U-Pb)||||Massive gabbro, bimodal magmatic and volcanic rocks including leucogranite, monzogranite, alkali-feldspar granite and alkali-feldspar syenite.|
73257|Warakurna Supersuite|68996|5|Briefly described|p5, 25, 28-29, 32, 35-47, 53, 54, 65,66|Mesoproterozoic|Mesoproterozoic|Age is of granite component. See also Warakurna granite p59.|1065 +/- 9 Ma||Includes Tollu granite, Winburn granite||Granites, quartz syenite, massive fine grained granodiorite, mylonitic syenogranite. Density ranges from 2.56->2.9g/cm^3.|
73257|Warakurna Supersuite|69003|5|Briefly described|p4, p37, p39, p49, p51-52, p59|Mesoproterozoic|Mesoproterozoic|W Musgrave Province, Paterson Orogen. Associated with Giles Orogeny. Includes the mainly felsic extrusive rocks of the Bentley Supergroup. Some units quarried for high-quality dimension stone.|||Giles intrusions.||Granite, gabbro, layered mafic-ultramafic intrusions.|
73257|Warakurna Supersuite|69009|5|Briefly described|Map Legend||||||Includes Alcurra Dolerite and Giles Suite.||Comprises layered mafic-ultramafic intrusions; magnetite; dolerite sills/dykes/plugs; granitic and rhyolitic rocks.|
73257|Warakurna Supersuite|69010|6|Mentioned|Map Legend|||Warakurna Large Igneous Province.|||Includes the Kulkatharra Dolerite.|||
73257|Warakurna Supersuite|69091|4|Described|p52 Fig.4.1, p53, see comments|Mesoproterozoic|Mesoproterozoic|Intrudes rocks of Musgrave Region (in geographical sense denotes general area in which Mesoproterozoic rocks of Musgrave Province outcrop). Formed during c. 1085 Ma to c. 1040 Ma Giles Event. Craton scale mafic magmatism (c. 1078-1073 Ma), basis for grouping igneous rocks into Warakurna Large Igneous Province (Wingate et al., 2004; Morris and Pirajno, 2005). Volcanic components of Warakurna Supersuite are grouped into Bentley Supergroup. See also Warakurna granite (p137 Fig.6.4 and p138 Fig.6.5). See also p54 Fig.4.2, p55 Fig.4.3, p58, p59 Fig.4.6, p69, p73 Fig.4.16, p82, p86, p131 Fig.6.1, p134 Fig.6.2, p141 Fig.6.8, p183, p205-206.|1085-1040 Ma||Kunmarnara Group, Bentley Supergroup, Giles Suite, Winburn Granite.||A-type granites; leucogranite, gabbro, layered mafic-ultramafic intrusions.|
73257|Warakurna Supersuite|69152|5|Briefly described|GEOL_LUT_CSV files + geochron files|Mesoproterozoic|Mesoproterozoic||||Includes Giles Suite|||
73257|Warakurna Supersuite|69153|5|Briefly described|GEOL_LUT_CSV files; GEOCHRON files|Mesoproterozoic|Mesoproterozoic|Tollu pluton' (185583) was dated (SHRIMP-B) at 1073+/-6 Ma, and is interpreted as the age of igneous crystallization of the granite. See GEOCHRON/194759.1.pdf, 194637.1.pdf and 185583.1.pdf.|||Alcurra Dolerite|is cross-cut by Kullal Dyke Suite; intrudes Wankanki Supersuite|Dolerite sill/plug, granite, syenogranite, leucogranite, (alkali feldspar/qtz) syenite, (cpx) granodiorite, hbl-bio-qtz monzodiorite to granodiorite, hbl-bio monzogranite and syenogranite, tonalite.|12-NOV-15
73257|Warakurna Supersuite|69166|6|Mentioned|geologyp_lut.csv|Neoproterozoic|Neoproterozoic||||Includes Kulkatharra Dolerite|||
73257|Warakurna Supersuite|69167|4|Described|geologyp_lut.csv|Mesoproterozoic|Mesoproterozoic|Age derived from dolerite sill sample (178187.1.pdf)|1050 +/- 22 Ma (SHRIMP)|||Intrudes Eel Creek Formation|Dolerite sill or plug; fine- to medium-grained dolerite and gabbro|
73257|Warakurna Supersuite|69185|5|Briefly described|500k_geologyp08_lut.csv|||Geological Province: Pilbara Craton.|||Includes Kilkatharra Dolerite.|||
73257|Warakurna Supersuite|69436|5|Briefly described|p21:1, 4, 10-12, 16|||Musgrave Province. Includes (Howard et al., 2011) all magmatic units formed during a second major phase of magmatism, during the Giles Event (1085-1040 Ma). Forms the Warakurna Large Igneous Province. Reworked by the Petermann Orogeny.|||Giles Complex, Alcurra Dolerite, Angatja Suite, Hull Suite, Michell Nob Granite, Nulchara Charnockite.||Mafic and ultramafic intrusive rocks.|12-JUL-16
73257|Warakurna Supersuite|69546|6|Mentioned|p115|Stenian|Stenian|Geological province: Musgrave Province. Associated with Giles Event.|1085-1040 Ma|||||
73257|Warakurna Supersuite|69554|6|Mentioned|p139|||Western Musgrave Province.|||||Orthogneisses.|
73257|Warakurna Supersuite|69583|5|Briefly described|p58, p82, p85, p92, p127; Plates 2, 3|Proterozoic|Proterozoic|Warakurna Large Igneous Province, northwestern and central Yilgarn Craton. Appears also on p58, p82 mis-spelt as Warrakuna Supersuite. Appears in seismic images as highly-reflective, shallow-dipping sills, hundreds of kilometres in extent and up to 200m thick.|c.1070 Ma.||Mount Holmes Gabbro.||Dolerite dykes, plugs and sills. Fine- to medium-grained dolerite and gabbro.|
73257|Warakurna Supersuite|69590|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Of Warakurna Large Igneous Province. Events: Warakurna Supersuite Magmatic Event. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 100k_geologyl_lut.csv, 250k_interpgeol_lut.csv.|1084-1047 Ma (inferred)||||Dolerite sill or plug; fine- to medium-grained dolerite and gabbro|
73257|Warakurna Supersuite|69596|6|Mentioned|p13||||||Kulkatharra Dolerite.|||
73257|Warakurna Supersuite|69655|5|Briefly described|p1-p2, p4-p5-p7, p57|Stenian|Stenian|Musgrave Province. Emplaced during the Giles event (which is the source of the age). Outcrops across approximately 1.5 million square kilometers in central and western Australia forming the Warakurna Large Igneous Province.|||Includes the Alcurra Dolerite.||Granites, gabbro and layered mafic-ultramic intrusions.|
73257|Warakurna Supersuite|69729|5|Briefly described|p68-69, p74 Fig.8, p75, p78-79, p81-82|||See also p66 Fig.1. Musgrave Province. This unit groups all the magmatic products of the c.1090-c.1040 Ma Giles Event. Bimodal volcanic rocks of this unit also form the main component of the Bentley Supergroup. Geochemistry detailed.|||||Granites, gabbro, layered mafic-ultramafic Giles intrusions.|
73257|Warakurna Supersuite|70083|6|Mentioned|p206-207|||Western Musgrave Inlier. Associated with the Giles Event.|1085-1040 Ma.||||Granites.|
73257|Warakurna Supersuite|70084|5|Briefly described|p220|Stenian|Stenian|Geological province: Musgrave Province, Paterson Orogen.|||Includes Bentley Supergroup.|||
73257|Warakurna Supersuite|70095|5|Briefly described|p17|||Geological province: Musgrave Province. Of Bentley Basin.|||Includes Bentley Supergroup, Winburn granite, Giles intrusions and Kunmarnara Group.|Overlain by Buldya Group.||
73257|Warakurna Supersuite|70132|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Warakurna Large Igneous Province.|1084-1067 Ma.||Kulkatharra Dolerite.|||
73257|Warakurna Supersuite|70134|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Bentley Basin. The five facies are mapped separately.|1078-1060 Ma.||Giles Suite.||Granitic rock, undivided; K-feldspar-phyric (to 5cm) quartz syenite, locally rapakivi textured; foliated hornblende-bearing syenogranite with mafic enclaves; leucocratic porphyritic to seriate syenogranite; coarse-grained tourmaline vein, foliated.|
73257|Warakurna Supersuite|70136|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Warakurna Large Igneous Province.|||Kulkatharra Dolerite.|||
73257|Warakurna Supersuite|70137|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic||1078-1062 Ma.|||Intrudes Frank Scott Formation (Mission Group), Scamp and Mount Waugh Formations.|Granitic rock, undivided; fine- to medium-grained quartz syenite containing K-feldspar phenocrysts up to 5cm, locally with rapakivi texture; dolerite sill or plug of fine- to medium-grained dolerite, and gabbro.|
73257|Warakurna Supersuite|70140|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Warakurna Large Igneous Province.|c.1070 Ma.||||Dolerite sill or plug; fine- to medium-grained dolerite and gabbro.|
73257|Warakurna Supersuite|70153|5|Briefly described|100k_geologyp10_lut.csv|Mesoproterozoic|Mesoproterozoic||||Includes Giles Suite.|||
73257|Warakurna Supersuite|70226|5|Briefly described|map legends|Mesoproterozoic|Mesoproterozoic|Warakurna Large Igneous Province.|1084-1047 Ma||||Dolerite sill or plug; fine- to medium-grained dolerite, and gabbro.|16-DEC-15
73257|Warakurna Supersuite|70419|5|Briefly described|p15-17, p23|Proterozoic|Proterozoic|Sills of this unit produce a highly reflective and gently N-dipping unit in seismic line 10GA-YU2. Appears as Warakurna Suite on p17.||||Correlates with Mount Holmes Gabbro.||
73257|Warakurna Supersuite|70619|5|Briefly described|map legend|Mesoproterozoic|Mesoproterozoic|Warkurna Large Igneous Province.|||Includes Giles Suite.||Granite; metagranite; amphibolite; gabbro; metagabbro.|03-JUN-16
73257|Warakurna Supersuite|70634|4|Described|100k_geologyp_lut,csv|Mesoproterozoic|Mesoproterozoic|Samples of granite (195231.1.pdf) are the sources for SHRIMP dates.|1055 Ma  (Isotopic)  1079 Ma +/- 8 Ma (SHRIMP)|Musgrave Complex|Includes Alcurra Dolerite, Giles Suite 1, Giles Suite 2, Giles Suite 1 (2), Bentley Supergroup|Intrudes into Wankanki Supersuite, Pitjantjatjara Supersuite|Granitic rock, quartz syenite, alkali feldspar granite, alkali feldspar quartz syenite, granodiorite, monzodiorite, monzogranite, pegmatitic leucogranite, mylonitic leucogranite, mylonitic syenogranite, syenogranite, tonalite, dolerite and gabbro.|
73257|Warakurna Supersuite|70763|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Warakurna Large Igneous Province.|||Giles Suite.|||
73257|Warakurna Supersuite|70767|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Warakurna Large Igneous Province.|||Kulkatharra Dolerite.|||
73257|Warakurna Supersuite|70768|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Warakurna Large Igneous Province.|||Kulkatharra Dolerite.|||
73257|Warakurna Supersuite|70770|5|Briefly described|Map legend.|Proterozoic|Proterozoic|Warakurna Large Igneous Province.|||||Dolerite sill or plug; fine- to medium-grained dolerite and gabbro.|
73257|Warakurna Supersuite|70793|4|Described|GEOL_LUT_CSV files + geochron files|Mesoproterozoic|Mesoproterozoic|Geological province: Musgrave Province. Of Warakurna Large Igneous Province. Includes all igneous and intrusive rocks of the 1093-1045 Ma Giles Event (Smithies et al., 2009). Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma); Warakurna Supersuite Magmatic Event (1084-1040 Ma); Giles Event (1085-1040 Ma). Sample GSWA 174589 (quartz syenite dyke) yielded an interpreted (weighted mean 207Pb*/206Pb*) crystallisation age of 1074+\-3 Ma for the syenite dyke. Sample GSWA 174662 (granophyre) yielded an interpreted (207Pb/206Pb concordia) magmatic crystallisation age of 1077+\-6 Ma. Sample GSWA 183474 (hornblende syenogranite) yielded an interpreted (207Pb/206Pb concordia) magmatic crystallisation age of 1072+\-8 Ma. Sample GSWA 183847 (syenite; also part of Kunmarnara Group) yielded an interpreted (regression intersecting concordia curve) magmatic crystallisation age of 1078+\-4 Ma. Sample GSWA 185509 (leucogranite) yielded an interpreted (weighted mean 207Pb*/206Pb*) magmatic crystallisation age of 1075+\-3 Ma. Sample GSWA 185583 (pophyritic granite) yielded an interpreted (regression itersecting concordia curve) igneous crystallisation date of 1073+\-6 Ma. Sample GSWA 187054 (quartz diorite) yielded an interpreted (207Pb*/206Pb* and 238U/206Pb* concordia) magmatic crystallisation age of 1055+\-10 Ma. Sample GSWA 187256 (granite dyke) yielded an interpreted (weighted mean 207Pb*/206Pb*) magmatic crystallisation age of 1066+\-9 Ma. Sample GSWA 189563 (hbl-bt syenogranite) yielded an interpreted (207Pb*/206Pb* and 238U/206Pb* concordia) igneous crystallisation age of 1065+\-9 Ma. See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop14_lut.csv, 100k_interpgeol_lut.csv, 500k_interpgeop_lut.csv, 100k_geologyl_lut.csv, 250k_interpgeol_lut.csv, 2_5m_interpgeop15_lut.csv, 500k_interpgeol_lut.csv, 2_5m_interpdykel15_lut.csv + other geochron files for additional geochronological analyses.|1084-1047 Ma (inferred)||Includes Alcurra Dolerite, Giles Suite.|Intrudes ino Wankanki and Pitjantjatjara supersuites.|Pegmatitic leucogranite, dolerite sill or pug, leucocratic tonalite, quartz syenite, syenogranite, monzogranite, rhyolite, granodiorite, granite.|
73257|Warakurna Supersuite|70794|5|Briefly described|2_5m_interpdykel15_lut.csv|Mesoproterozoic|Mesoproterozoic|Warakurna Large Igneous Province|1084-1047 Ma inferred||||Dolerite sill or plug, fine to medium grained dolerite and gabbro.|
73257|Warakurna Supersuite|70795|4|Described|2_5m_interpdykel15_lut.csv|Mesoproterozoic|Mesoproterozoic|Also 2_5m_interpgeop15_lut.csv|1084-1047 Ma||Includes Kulkatharra Dolerite||Dolerite sill or plugs, fine-medium grained dolerite, gabbro. Layered mafic-ultramafic intrusions, massive gabbro, granite and associated mafic to felsic volcanic rocks.|
73257|Warakurna Supersuite|70796|4|Described|2_5m_interpgeop15_lut.csv|Mesoproterozoic|Mesoproterozoic|Of the Warakurna Large Igneous Province. Affected by the following events: Alice Springs Orogeny (450  295 Ma); Petermann Orogeny (580  520 Ma); Paterson Orogeny (635  540 Ma); Warakurna Supersuite Magmatic Event (1084  1040 Ma); Giles Event (1090  1040 Ma). An inferred minimum age of 1040 Ma is also provided. See also 2_5m_interpdykel15_lut.csv, 100k_geologyl_lut.csv, 100k_interpgeol_lut.csv, 500k_interpgeol_lut.csv, 500k_interpgeop14_lut.csv, Bungar100_2539_stratig.pdf, Yalgoo100_2241_stratig.pdf, Youanmi100_2640_stratig.pdf.|1084 +/ 9 Ma (Max age, isotopic)||||Layered maficultramafic intrusions, massive gabbro, granite, and associated mafic to felsic volcanic rocks. Diorite, minor syenogranite, dolerite sill or plug.|
73257|Warakurna Supersuite|70814|6|Mentioned|p37||||||||Mafic magmas.|
73257|Warakurna Supersuite|70826|6|Mentioned|p10, p14 tbl 5|Mesoproterozoic|Mesoproterozoic|Capricorn Orogen, Musgrave Province, Yilgarn Craton.|1084-1047 Ma||Giles Suite, Alcurra Dolerite, Kulkatharra Dolerite, Prenti Dolerite||Mafic and locally felsic igneous rocks.|
73257|Warakurna Supersuite|70830|5|Briefly described|p22, p40|Stenian|Stenian|Youanmi Terrane. Misspelt as the Warakurna Suite on p40.|c. 1070 Ma|||||
73257|Warakurna Supersuite|70831|5|Briefly described|p2, p5-p6, p9|Stenian|Stenian|Musgrave Province.|c. 1085-1040 Ma||Includes the Alcurra Dolerite.||Layered mafic and ultramafic intrusions, mixed and mingled gabbros and leucogranites and bimodal volcanics.|
73257|Warakurna Supersuite|70839|5|Briefly described|p326-327,336,339,341-342,345|Stenian|Stenian|Geological province: Musgrave Province. Voluminous mafic and felsic mantle-derived intrusive and extrusive magmatic rocks associated with c. 1.09-1.04 Ga Giles Event (Smithies et al., 2015). Emplaced within Ngaanyatjarra Rift (Evins et al., 2010; Aitken et al., 2012).|c. 1.09-1.04 Ga||Includes Kunmarnara Group.|Underlain by, and interbedded with Kunmarnara Group and Bentley Supergroup.|Mafic and felsic intrusives and extrusives; sediments.|
73257|Warakurna Supersuite|71088|5|Briefly described|p4-p5, p25|||Musgrave Region. Mantle-derived.|1090-1040 Ma|||Overlies and interbeds with the Kunmarnara Group and Bentley Supergroup.|Mafic and felsic, intrusive and extrusive igneous rocks.|
73257|Warakurna Supersuite|71158|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Warakurna Large Igneous Province.|1084-1067 Ma.|||||
73257|Warakurna Supersuite|71159|5|Briefly described|Map legend.|Proterozoic|Proterozoic|Warakurna Large Igneous Province. The two facies are mapped separately.|||||Diorite to minor syenogranite in dykes and sills; dolerite sill or plug: fine- to medium-grained dolerite, and gabbro.|
73257|Warakurna Supersuite|71169|5|Briefly described|p81-p82|Stenian|Stenian|Musgrave Province. |1085-1040 Ma||||Dolerite sills.|
73257|Warakurna Supersuite|71170|5|Briefly described|p5-p6|||Emplaced during the Giles Event.|||||Gabbro, granites and layered mafic-ultramafic intrusions.|
73257|Warakurna Supersuite|71210|6|Mentioned|xv, p8, p20, p97, p99, p112, p131, p134|||Musgrave Province.|c. 1090 - 1040 Ma||Includes the Giles Suite.|||
73257|Warakurna Supersuite|71211|6|Mentioned|p6, p7 fig 1.4, p10, p24 fig 2.1|||See also  p84 fig 3.1, p85, p136 fig 4.1, p216, p231.|||||Granites, gabbros and layered mafic-ultramafic intrusions.|
73257|Warakurna Supersuite|71268|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Of Warakurna Large Igneous Province. Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma); Warakurna Supersuite Magmatic Event (1084-1040 Ma); Giles Event (1085-1040 Ma). Sample GSWA 174662 (granophyre) yielded a concordia age of 1077+\-6 Ma, interpreted as the magmatic crystallization age of the granophyre. Sample GSWA 174761 (porphyritic granite dyke) yielded a weighted mean 207Pb/206Pb date of 1075+\-7 Ma, interpreted as the magmatic crystallization age of the granite dyke. Sample GSWA 183474 (hbl syenogranite) yielded a concordia intercept date of 1072+\-8 Ma, interpreted to be magmatic crystallisation age. Sample GSWA 185486 (porphyritic microgranite) yielded a concordia age of 1072+\-5 Ma, interpreted as magmatic crystallisation age of the microgranite. Sample GSWA 185509 (leucogranite) yielded a weight mean 207Pb/206Pb age of 1075+\-3 Ma, interpreted to be magmatic crystallisation age. Sample GSWA 185583 (k-spar granite) yielded a regression intersecting concordia curve at 1073+\-6 Ma ,interpreted as igneous crystallisation age. Sample GSWA 208453 (syenogranite) yielded a regression intersecting concordia curve at 1063+\-8 Ma, interpreted as magmatic crystallisation age of the syenogranite. Sample GSWA 208486 (migmatitic metasyenogranite) yielded a weighted mean 207Pb/206Pb age of 1031+\-6 Ma, interpreted as magmatic crystallisation age. See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeop16_lut.csv, 100k_interpgeol_lut.csv, 100k_geologyl_lut.csv, 250k_interpgeol_lut.csv, 2_5m_interpgeop15_lut.csv, 500k_interpgeol_lut.csv, 2_5m_interpdykel15_lut.csv.|1084-1047 Ma (inferred)||Includes Alcurra Dolerite, Giles Suite.||Pegmatitic leucogranite, dolerite sills and gabbro, tonalite, syenite, syengogranite, monzogranite, granite, leucogranite; metamorphosed.|
73257|Warakurna Supersuite|71269|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Of Warakurna Large igneous Province. Events: Alice Springs Orogeny (450 - 295 Ma); Petermann Orogeny (580 - 520 Ma); Paterson Orogeny (635 - 540 Ma); Warakurna Supersuite Magmatic Event (1084 - 1040 Ma); Giles Event (1085 - 1040 Ma). See 500k_interpgeol_lut.csv, 2_5m_interpgeop15_lut.csv, 2_5m_interpdykel15_lut.csv.|1084-1040 Ma (inferred)||||Diorite to minor syenogranite in dykes and sills; dolerite sill or plug; fine- to medium-grained dolerite, and gabbro.|
73257|Warakurna Supersuite|71270|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Geological province: Kepa Kurl Booya Province, Albany-Fraser Orogen, West Australian Craton. Events: Albany-Fraser Orogeny Stage II (1225 - 1140 Ma); Albany-Fraser Orogeny (1330 - 1140 Ma); Albany-Fraser Orogeny Stage I (1330 - 1260 Ma); Biranup Orogeny (1710 - 1650 Ma); Ngadju Event (1780 - 1760 Ma); Salmon Gums Event (1815 - 1800 Ma); Tropicana Event (2520 - 2505 Ma); Atlantis Event (2720 - 2550 Ma). See 100k_geologyp10_lut.csv, 500k_interpgeop16_lut.csv, 100k_geologyp14_lut.csv, 500k_interpgeop_lut.csv, 2_5m_interpgeop15_lut.csv, 2_5m_interpdykel15_lut.csv.|1084+\-9 Ma; 1040 Ma||Includes Giles Suite, Prenti Dolerite.||Layered mafic-ultramafic intrusions, massive gabbro, granite, and associated mafic to felsic volcanic rocks.|
73257|Warakurna Supersuite|71321|6|Mentioned|p5|Stenian|Stenian|Geological province: Musgrave Province.|1085-1040 Ma|||||
73257|Warakurna Supersuite|71416|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Warakurna Large Igneous Province.||||||
73257|Warakurna Supersuite|71592|5|Briefly described|Appendix A.|||Musgrave Province.|1074+/-3 Ma (crystallisation: U-Pb zircon).||||Microgranite, rhyolite, quartz syenite dyke.|
73257|Warakurna Supersuite|71891|6|Mentioned|p8|||||||||
73257|Warakurna Supersuite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoproterozoic|Mesoproterozoic||max age 1084+/-6 Ma, min age ~1040 Ma inferred.||Includes Giles Suite 1, Giles Suite 2.||Layered mafic-ultramafic intrusions, massive gabbro, granite, + associated mafic to felsic volcanic rocks; Dolerite sill/plug; fine- to medium-grained dolerite, and gabbro; Strongly foliated biotite metamonzogranite; medium-grained; equigranular;|
73257|Warakurna Supersuite|72094|4|Described|p2, p3, 4, 12, 13, 14, p15-16, 17, 18|Stenian|Stenian|Musgrave Province.  Suite of igneous rocks associated with Giles event. Intrudes Mount Palgrave and Pussy Cat Groups, and U-Pb magmatic crystallization zircon ages of 1071+/-5, 1063+/-8 and 1049+/-8 Ma suggest that Warakurna Supersuite intruded and formed source of volcano-sedimentary succession in Talbot Sub-basin. Summary table of zircon geochronology on p8 Table 1.  Reference made to Warakurna Large Igneous Province on p17. Associated with Giles Event Stage 3 3.|c. 1071+/-5 - 1031+/-6 Ma||Includes Giles intrusions, G2 gabbros, Alcurra Dolerite intrusions and bimodal volcanic rocks of the Talbot Supervolcano.|Unconformably overlain by Cobb Embayment sediments. Intrudes Talbot Sub-basin rocks.|Quartz, synenite and syenogranitic rocks. Dolerite, gabbro, layered mafic-ultramafic intrusions.|
73257|Warakurna Supersuite|72242|5|Briefly described|p29-30,32|Stenian|Stenian|Geological province: Coompana Province, Western Gawler Craton. Includes a massive olivine dolerite and microgabbro drilled in CDP002, dated at 1074+\-6 Ma (magmatic crystallisation age; Jagodzinski and Bodorkos 2018).|1078-1070 Ma||Includes Mallabie Volcanics and Gaints Head Suite.|||
73257|Warakurna Supersuite|72344|5|Briefly described|p3, p7-p9, p35, p44|||Coompana Province. Petrography, SHRIMP analyses and geochemistry are discussed for several samples. See also p143.|||Includes the Mallabie Volcanics and Giants Head Suite.|||
73257|Warakurna Supersuite|72443|5|Briefly described|p737-738||||||Includes the Alcurra Dolerite and the Winburn Granite.|||
73257|Warakurna Supersuite|72934|6|Mentioned|p4, p11-12, App.A|||Yielded a U-Pb SIMS zircon magmatic crystallisation age of 1074 +/- 6 Ma. Part of the Warakurna large igneous province/Ngaanyatjarra Rift[?].||||||
73257|Warakurna Supersuite|72947|6|Mentioned|p8-9, p17, p19-20|Stenian|Stenian|Of the Warakurna Large Igneous Province. Suggested to be contemporaneous with the Giants Head and Warbla Suites, extending the LIP over 400 km south, into the Coompana Province .|c. 1085 - 1030 Ma||Warbla Basalt[?], Warbla Suite, Giants Head Suite.|||
73257|Warakurna Supersuite|73058|5|Briefly described|p761 Fig.1, p768-769, p771-772, p774-776|Stenian|Stenian|Musgrave Province. Formed the Warakurna Large Igneous Province during the c.1075 Ma Giles Event, c. 10km thick sequence of bimodal volcanic rocks. Felsic rocks are strongly ferroan and alkalic-calcic, extreme enrichments in REE and HFSE. Nd model ages suggest mantle extraction event at 1700 Ma. Inferred additional significant juvenile mantle additions are masked in Hf isotope record by HFSE enriched crustal sources. Location in text includes p773 Tb.5, p777 Fig.14.|c. 1085-1040 Ma||Giles intrusions||Includes mafic-felsic volcanic rocks, layered mafic-ultramafic intrusions, granites, gabbros, and minor sedimentary rocks, local ultramafic cumulates.|
73257|Warakurna Supersuite|73091|6|Mentioned|Mapsheet||||||Includes the Giants Head Suite.|||
73257|Warakurna Supersuite|73177|5|Briefly described|p1100, 1114 Fig.16|||Musgrave Province.|1085-1050 Ma.|||||
73257|Warakurna Supersuite|73224|6|Mentioned|p42|Stenian|Stenian||c. 1074 Ma||Giants Head Suite, Mallabie Basalt, Warbla Suite|||
73257|Warakurna Supersuite|73225|5|Briefly described|p4||||c.1074 Ma.||Giants Head Suite, Warbla Suite, Mallabie Basalt.|||
73257|Warakurna Supersuite|73234|6|Mentioned|p19|Stenian|Stenian|Musgrave Province.|c. 1090-1040 Ma||||Includes igneous rocks.|
73257|Warakurna Supersuite|73346|6|Mentioned|p1-2, p4-6, p25|Mesoproterozoic|Mesoproterozoic|Produced during the 1085-1030 Ma Giles Event.|||||Includes mafic and felsic intrusive and extrusive magmatic rocks.|
73257|Warakurna Supersuite|73410|5|Briefly described|p7, 12|||Murchison Domain, Yilgarn Craton.|c.1075 Ma.||||East-striking, 50-150 km-long mafic, including dolerite, dykes.|
73257|Warakurna Supersuite|73437|5|Briefly described|p151, p153|Mesoproterozoic|Mesoproterozoic|Contains igneous rocks formed during the Giles Event.|||Giles Suite, West Hinckley Suite, Alcurra Dolerite||Igneous rocks including layered mafic-ultramafic intrusions, mixed and mingled gabbros and leucogranites, granite and dolerite intrusions, bimodal volcanic rocks.|
73257|Warakurna Supersuite|73641|6|Mentioned|p4||||||Warbla, Giants Head Suites; Mallabie Basalt.|||
73257|Warakurna Supersuite|74367|6|Mentioned|p23|||Musgrave Province.||||||
80746|Warbla Basalt|72344|5|Briefly described|p7|Stenian|Stenian|Coompana Province. Intersected in drillholes CDPO07, BN1 and BN2.|c. 1074 Ma|Giants Head Suite|||Two pyroxene basalt.|
80746|Warbla Basalt|72947|6|Mentioned|p8 Fig.3|||[Possibly meaning Warbla Suite] See Figure 3 legend.||Warakurna Supersuite||||
82823|Warbla Suite|72947|2|Defined|p7, p9, p18, p20-21|Stenian|Stenian|Coompana Province, southeastern. Named after Warbla Cave. No known surface exposures. Type locality: CDP007 (drillhole 299061, interval 310.80-351.31 m). Product of mantle melting derived from heterogeneous lithospheric mantle. Evolved (strongly negative) eHf1074 Ma values indicating contamination by a 1900 Ma crust. Similar relative timing relations and the same remnant magnetic signature as the Giants Head Suite and Mallabie Basalt but geochemically distinct from the Giants Head Suite; suggests they are not genetically related and had different sources. Derived from the same modified lithospheric mantle source that produced the Merdayerrah Shoshonite. Known from a small, north-south aligned <1 by <0.5 km intrusive body and a weakly elongate 2 by 3 km east-northeast aligned body; thus, it is difficult to confidently assign similar undrilled bodies to either the Giants Head or Warbla suites.|c. 1074 Ma|Warakurna Supersuite||Intrudes Koomalboogurra Suite and Koonalda Suite.|Pyroxene-bearing (olivine-absent) volcanic to subvolcanic rocks, including dark grey, fine- to medium-grained, massive and inequigranular to weakly porphyritic basalts and dolerites.|
82823|Warbla Suite|73224|5|Briefly described|p42|Stenian|Stenian|Produced from intraplate magmatism; result from melting heterogeneous lithospheric mantle.|c. 1074 Ma|Warakurna Supersuite||||
82823|Warbla Suite|73225|5|Briefly described|p4||||c.1074 Ma.|Warakurna Supersuite.||Correlated with Giles Complex.|Intrusive and extrusive mafic magmatism.|
82823|Warbla Suite|73641|6|Mentioned|p4|||||Warakurna Supersuite||||
27953|Warcowie Dolomite Member|22510|5|Briefly described|table1p37|||Of the Wilyerpa Formation.  Age: Sturtian. Mid-North Region.||||||13-OCT-04
27953|Warcowie Dolomite Member|39344|6|Mentioned|Map legend|Precambrian|Precambrian|Sturtian||||||
27953|Warcowie Dolomite Member|39348|6|Mentioned|Map legend|Precambrian|Precambrian|Sturtian||||||
27953|Warcowie Dolomite Member|40225|6|Mentioned|Map sheet|||||||||
27953|Warcowie Dolomite Member|40294|3|Fully described|p43|||||||||
27953|Warcowie Dolomite Member|41405|3|Fully described|p159|||||||||
27953|Warcowie Dolomite Member|42720|6|Mentioned|map legend|Sturtian||||||||
27953|Warcowie Dolomite Member|42813|6|Mentioned|p20|||of Wilyerpa Formation||||||
27953|Warcowie Dolomite Member|42882|5|Briefly described|p5, Table 1 p3|||of Wilyerpie Formation||||||
27953|Warcowie Dolomite Member|43052|5|Briefly described|p183,Table 6.1|||||||||
27953|Warcowie Dolomite Member|60959|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Of the Wilyerpa Formation. Sandy and pebbly dolomite, conglomerate, minor diamictite.||||||
27953|Warcowie Dolomite Member|61732|5|Briefly described|p28 Fig. 13|Sturtian|Sturtian|Of the Wilyerpa Formation (Yudnamutana Subgroup, Umberatana Group). Geological Province: Adelaide Rift Complex.||||||07-FEB-11
27953|Warcowie Dolomite Member|65925|5|Briefly described|Appendix 2.||||||||Conglomerate, massive, well rounded pebble and boulder clasts, silty and sandy matrix; dolomite, massive to well bedded, grey and brown; breccia, dolomitic matrix.|
27953|Warcowie Dolomite Member|70031|5|Briefly described|p245|Cryogenian|Cryogenian|Adelaide Geosyncline. Associated with Sturtian glaciation.||Unit of Wilyerpa Formation.||Overlain by Wilyerpa Formation. Underlain by Benda Siltstone and Holowilena Ironstone.||
27953|Warcowie Dolomite Member|70323|5|Briefly described|p219|Cryogenian|Cryogenian|Central Flinders Ranges, Adelaide Geosyncline. Thickness: ~2m.||Unit of Wilyerpa Formation.||Underlain by Holowilena Ironstone.|Dolomite.|
77404|Ward Volcanics|65376|6|Mentioned|p10. ||||c.1650 Ma.|||||
39175|Wardang Volcanics Member|24475|2|Defined|p54|Paleoproterozoic|Paleoproterozoic|Of Weetulta Formation. Formerly Wardang Volcanics.||||||07-NOV-08
39175|Wardang Volcanics Member|60958|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Weetulta Formation. Red-brown porphyritic rhyolite, rhyodacite, dacite to latite. A Type, foliated. Age: 1756 +/- 27Ma. Geological Province: Gawler Craton.||||||07-NOV-08
39175|Wardang Volcanics Member|61121|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of Weetulta Fm. Red-brown porphyritic rhyolite, rhyodacite, dacite to latite, mainly K-feldspar, quartz, plagioclase, biotite, opaques, hornblende, pyroxenes, chlorite, epidote. Age: ~1800Ma. Geological Province: Gawler Craton.||||||09-JUL-13
39175|Wardang Volcanics Member|65375|4|Described|pp19-20, pp22-23, p47.|||Average SiO2 of 69.46%. Phenocrysts and matrix predominantly K-feldspar. Intercalates with, or intrudes, conglomerate and tuffaceous siltstone of Aagot Member.|1756 +/- 27 Ma.|Unit in Weetulta Formation.|||Massive porphyritic rhyodacite, dacite or latite, locally rhyolite; K-feldspar or calc-plagioclase phenocrysts; local flow banding, columnar cooling structures, hyaloclastics and chaotic flow folding.|
39175|Wardang Volcanics Member|65376|4|Described|pp110-111.|||Type section on Wardang Island. Widespread peperite development suggests volcanism was contemporaneous with sedimentation. Dating imprecision does not enable distinction from Moonta Porphyry Member as a separate magmatic event.|1772 +/- 14 Ma.|Unit in Weetulta Formation.||Interfingers with and intrudes Aagot Member.|Plagioclase-phyric rhyodacite, dacite and latite; locally rhyolite.|
39175|Wardang Volcanics Member|66302|6|Mentioned|p29, p33|Statherian|Statherian|Olympic Domain, Gawler Craton. Igneous extrusive age. |1772 +/- 14 Ma (Fanning et al, 2007)|Weetulta Formation||||
39175|Wardang Volcanics Member|67181|5|Briefly described|p629|Statherian|Statherian|Gawler Craton. 1772 +/- 14 Ma from Fanning et al. (2007)|1772 +/- 14 Ma|Unit in Weetulta Formation.||||
39175|Wardang Volcanics Member|69748|5|Briefly described|p179-182, 188|Paleoproterozoic|Paleoproterozoic|Moonta-Wallaroo region, Olympic IOGC Province. Is presented as Wardang Volcanic Member; the ""Member"" component of the name is, more often than not, omitted.|~1740 Ma.|Weetulta Formation.|||Fine-grained, flow-banded texture. Predominantly composed of K-feldspar, quartz, minor albite; contains abundant hematite and accessory apatite.|
39175|Wardang Volcanics Member|73092|6|Mentioned|p19|Statherian|Orosirian|Age is of magmatic crystallisation. Dated sample is rhyodacite from Port Victoria. This age is within uncertainty of the previous age for the Wardang Volcanics. [Note that ASUD lists that Wardang Volcanics was superseded by Wardang Volcanics Member].|1779 +/- 31 Ma|Wallaroo Group|||Rhyodacite to dacite volcanic rocks, with extrusive features, peperite and local contemporaneous sedimentation.|
39175|Wardang Volcanics Member|73155|6|Mentioned|p281 Fig.12|||||Wallaroo Group||||
29118|Warragee Member|35835|2|Defined|p198|Middle Cambrian|Early Cambrian|Lower to Middle Cambrian||||||
29118|Warragee Member|35954|6|Mentioned|p1229|||See also Fig.2.||||||
29118|Warragee Member|36495|6|Mentioned|p129|||||||||
29118|Warragee Member|37326|6|Mentioned|p3|||||||||
29118|Warragee Member|37802|6|Mentioned|Fig.2|||||||||
29118|Warragee Member|42269|6|Mentioned|p336|||||||||
29118|Warragee Member|60889|5|Briefly described|p247 Fig.4|Early Cambrian|Early Cambrian|||Billy Creek Formation||||
29118|Warragee Member|62270|5|Briefly described|p496, p502, p509 Fig. 8|Early Cambrian|Early Cambrian|Of the Billy Creek Formation. Contains fossil trilobites.||||||
29118|Warragee Member|63569|6|Mentioned|p122|||||Of lower Billy Creek Formation||||
29118|Warragee Member|65892|5|Briefly described|p28.|Early Cambrian|Early Cambrian|Of Moore (1979). Includes emuellid trilobite Balcoracania dailyi.||Unit in Billy Creek Formation.||Conformably overlies Edeowie Limestone Member.|Red, green and grey shale interbedded with fine- to medium-grained siltstone; minor interbeds of dolomite, tuff, coarse siltstone.|
29118|Warragee Member|65925|6|Mentioned|p14 Fig.2.2.|Early Cambrian|Early Cambrian|||||||
81330|Warramboo magnetite gneiss|70027|3|Fully described|p56-57,59,61, 70-73|Neoarchean|Neoarchean|Geological province: Gawler Craton. Prominent high response on aeromagnetic imagery with east west-trending fabrics. Metamorphosed to upper amphibolite or granulite facies, producing a coarse-grained gneiss and upgrading the Warramboo iron deposit from BIF to  economic deposit. Isoclinally folded and interlayered with Sleaford Complex metasedimentary and meta-igneous gneisses. Derived from sedimentary protoliths based on aluminosilicate mineralogy and heterogeneous nature of magnetite gneisses in drill core. Zircon U-Pb SHRIMP geochronology detailed on p61-70; Sm-Nd whole rock data detailed on p70-71. Sm-Nd whole rock ages includes 1766+\-6, 1753+\-8 and 1749+\-5 Ma. Youngest detrital zircon populations range in age from 1766 Ma to 1742 Ma. Protolith minimum depositional age constrained by growth of ca. 1730 rims. Time gap between deposition and metamorphism is possibly <20My. Zircon provenance is dominated by ca. 1790-1750 Ma zircon, likely sourced from various igneous rocks of the Gawler Craton. Coeval with Wallaroo Group, Moonabie Formation, and significantly, Price Metasediments (similar U-Pb zircon and Sm-Nd isotopic data). Likely a similar sedimentary source to the Price Metasediments, based on presence of spessartine garnet; and probably formed in the same basin system. Probably correlable to Cape Hunter phyllite (Antarctica).|ca. 1750 Ma|||Compared to Price Metasediments.|Magnetite+\-hematite-biotite-K-feldspar-quartz migmatitic gneiss, magnetite-garnet-sillimanite-cordierite-biotite-K-feldspar quartz gneiss and magnetite-hematite-biotite-quartz-K-feldspar gneiss.|09-AUG-19
26203|Warren Schist|31292|2|Defined|p20|early Adelaidean|early Adelaidean|See also P21Prob.Lower Adelaidean||||||
24564|Warrina Supergroup|22772|5|Briefly described|p63,Table13.1|Cryogenian|Cryogenian|||||||
24564|Warrina Supergroup|22857|5|Briefly described|p63, Tb. 13.1 (insert p70-71)|Cryogenian|Cryogenian|Comprises the Burra and Callanna Groups. Age: 850-700Ma.||||||09-MAR-06
24564|Warrina Supergroup|23205|6|Mentioned|p133|||of Adelaide Geosyncline.||||||
24564|Warrina Supergroup|23516|5|Briefly described|p599 Fig.5|Neoproterozoic|Neoproterozoic|||||||
24564|Warrina Supergroup|24175|6|Mentioned|p6|Neoproterozoic|Neoproterozoic|||||||
24564|Warrina Supergroup|24586|5|Briefly described|p51 Fig. 2|Adelaidean|Adelaidean|Includes the Burra and Callanna Groups. Geological Province: Adelaide Geosyncline.||||||
24564|Warrina Supergroup|38004|2|Defined|p82|Precambrian|Precambrian|||||||
24564|Warrina Supergroup|38703|6|Mentioned|p131|||||||||
24564|Warrina Supergroup|38704|6|Mentioned|p133|||||||||
24564|Warrina Supergroup|39344|6|Mentioned|Map legend|Precambrian|Adelaidean|Willouran to Sturtian||||||
24564|Warrina Supergroup|40763|6|Mentioned|p204|||||||||
24564|Warrina Supergroup|41364|6|Mentioned|Fig.1|||||||||
24564|Warrina Supergroup|41401|5|Briefly described|p32|||||||||
24564|Warrina Supergroup|41404|6|Mentioned|p73|||||||||
24564|Warrina Supergroup|41405|6|Mentioned|p126|||||||||
24564|Warrina Supergroup|41647|6|Mentioned|Fig.2|||||||||
24564|Warrina Supergroup|41770|6|Mentioned|Fig.1|||||||||
24564|Warrina Supergroup|42011|6|Mentioned|Fig.2 P457|||||||||
24564|Warrina Supergroup|42028|6|Mentioned|p137|||||||||
24564|Warrina Supergroup|42215|6|Mentioned|Fig.2 P448|||||||||
24564|Warrina Supergroup|42238|6|Mentioned|p71|||||||||
24564|Warrina Supergroup|42239|6|Mentioned|Fig.2 P151|||||||||
24564|Warrina Supergroup|42882|5|Briefly described|Table 1, p3|||||||||23-JAN-19
24564|Warrina Supergroup|43052|5|Briefly described|p172|||formed of Callanna and Burra Groups||||||
24564|Warrina Supergroup|43595|5|Briefly described|p543-545||Neoproterozoic|||||||
24564|Warrina Supergroup|43845|5|Briefly described|Fig2 p42||Neoproterozoic|||||||12-JUL-16
24564|Warrina Supergroup|60959|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Includes: Callanna Group, Burra Group.||||||
24564|Warrina Supergroup|62592|5|Briefly described|p50 Table 5.1|Sturtian|Willouran|Adelaide Geosyncline.|||Includes Callanna and Burra Groups.|||
24564|Warrina Supergroup|62664|6|Mentioned|p138 Fig.2.|Neoproterozoic|Neoproterozoic||||Includes Callanna and Burra Groups.|||
24564|Warrina Supergroup|64796|6|Mentioned|p185, p190-191|Neoproterozoic|Neoproterozoic|Of Adelaide Rift Complex.|||Includes Callanna and Burra Groups.|||
24564|Warrina Supergroup|64801|6|Mentioned|p110|Neoproterozoic|Neoproterozoic|Adelaide Rift Complex.|||Callanna, Burra Groups.|Is overlain by Heysen Supergroup.||
24564|Warrina Supergroup|65376|5|Briefly described|p9 Fig.1.2. |Neoproterozoic|Neoproterozoic||||||Evaporitic, fluvial and marine sediments, diapiric breccia, minor volcanics.|
24564|Warrina Supergroup|65379|5|Briefly described|p643|Neoproterozoic|Neoproterozoic|Includes Burra Group. A major stratigraphic subdivision of the Adelaide Geosyncline.||||||07-MAR-12
24564|Warrina Supergroup|66884|6|Mentioned|p41 Fig.3|||[Mis-spelt as Warinna].|||Burra Group|||
24564|Warrina Supergroup|68030|6|Mentioned|p236, p238|||Flinders Ranges.|||Includes Burra and Callana groups.|Overlain by the Heysen Supergroup.||26-JUN-19
24564|Warrina Supergroup|68131|5|Briefly described|p2 Fig.1|Neoproterozoic|Neoproterozoic|Evaporitic, fluvial and marine deposits.|||||Sedimentary rocks, diapiric breccia, minor volcanics.|
24564|Warrina Supergroup|70384|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Adelaide Geosyncline. Age shown more specifically as Torrensian [Cryogenian].|||Includes Callanna, Burra Groups.|Is overlain unconformably by Heysen Supergroup.||23-JAN-19
24564|Warrina Supergroup|70407|5|Briefly described|p102 Fig 1, p103 Fig 2|Neoproterozoic|Neoproterozoic|Age: Willouran - Torrensian|||Includes Callanna Group, Burra Group.|||
24564|Warrina Supergroup|71268|5|Briefly described|1m_geologyp12_lut.csv||||||Includes Callanna Group.|||
24564|Warrina Supergroup|71593|5|Briefly described|p20|Neoproterozoic|Neoproterozoic|Gawler Craton.||||Overlain by the Heysen Supergroup.||
24564|Warrina Supergroup|73222|6|Mentioned|p6|Tonian|Tonian|Adelaide Rift Complex.|||Burra Group, Callanna Group, and units therein|||
24564|Warrina Supergroup|73262|6|Mentioned|p583|[Tonian?]|[Tonian?]|||||||
24564|Warrina Supergroup|74367|5|Briefly described|p4, p6|Tonian|Tonian|Early rift sequences. Largely restricted to depositional fault-bound troughs.|||Callanna Group, Burra Group||Dominated by clastic and carbonate rocks.|
23149|Warrindi Silt|44133|5|Briefly described|p164, 152 Fig. 10.2|Oligocene|Oligocene|Geological Province: Saint Vincent Basin. Thickness: 20m. ||||||
25753|Warrow Quartzite|22629|6|Mentioned|p149|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
25753|Warrow Quartzite|23285|4|Described|p 335|||Parent: Hutchison Group||||||
25753|Warrow Quartzite|23491|6|Mentioned|p18|||Of Hutchison Group.   Unconformably overlies the Kiana Granite.||||||
25753|Warrow Quartzite|23719|4|Described|p12|Paleoproterozoic|Paleoproterozoic|See also page 14 table 1. Of Hutchinson Group. Overlain by Middleback Subgroup. Geological Province Gawler Craton. Max. thickness: 500 m.||||||02-JUN-09
25753|Warrow Quartzite|23818|5|Briefly described|p27 Fig.6|||Of the Cleve Metamorphics. Max. thickness: ~12 000 ft. Geological Province: Gawler Block.||||||
25753|Warrow Quartzite|24365|6|Mentioned|p4|||Of the Hutchison Group.||||||
25753|Warrow Quartzite|31034|6|Mentioned|p130|||||||||
25753|Warrow Quartzite|32400|6|Mentioned|p91|||Geophysics. Archaean?||||||
25753|Warrow Quartzite|32428|6|Mentioned|p99|||||||||
25753|Warrow Quartzite|32429|6|Mentioned|p92|||||||||
25753|Warrow Quartzite|32435|5|Briefly described|p111|||||||||
25753|Warrow Quartzite|32930|6|Mentioned|p26|||Archaean||||||
25753|Warrow Quartzite|33466|6|Mentioned|Map legend|Archean|Archean|||||||07-NOV-08
25753|Warrow Quartzite|33470|4|Described|p462|||||||||
25753|Warrow Quartzite|34537|4|Described|p28|||||||||
25753|Warrow Quartzite|35255|6|Mentioned|p7|||||||||
25753|Warrow Quartzite|35672|6|Mentioned|p9|||||||||
25753|Warrow Quartzite|37461|5|Briefly described|p316|||||||||
25753|Warrow Quartzite|37620|6|Mentioned|p7|||||||||
25753|Warrow Quartzite|37811|1|Redefined|p237|Paleoproterozoic|Paleoproterozoic|See aslo Fig.2||||||07-NOV-08
25753|Warrow Quartzite|38969|6|Mentioned|p220|||||||||
25753|Warrow Quartzite|39345|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
25753|Warrow Quartzite|39349|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
25753|Warrow Quartzite|39352|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
25753|Warrow Quartzite|39353|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
25753|Warrow Quartzite|40227|6|Mentioned|Fig.2|||||||||
25753|Warrow Quartzite|40430|6|Mentioned|p7|||||||||
25753|Warrow Quartzite|40448|5|Briefly described|p27|||||||||
25753|Warrow Quartzite|40644|5|Briefly described|p120, p128||Mesoproterozoic|A thick quartzite unit in the Middleback Range - containing local quartz-pebble conglomerate beds. Age: <ca. 2300Ma.||||||13-AUG-08
25753|Warrow Quartzite|40983|6|Mentioned|p374|||||||||
25753|Warrow Quartzite|41325|6|Mentioned|Fig.2|||||||||
25753|Warrow Quartzite|41327|6|Mentioned|p3|||||||||
25753|Warrow Quartzite|41619|6|Mentioned|Map legend|Holocene||||||||
25753|Warrow Quartzite|41667|5|Briefly described|p5|||||||||
25753|Warrow Quartzite|41972|5|Briefly described|p365|||||||||
25753|Warrow Quartzite|42283|6|Mentioned|p80|||||||||
25753|Warrow Quartzite|42546|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
25753|Warrow Quartzite|42736|5|Briefly described|map legend|Paleoproterozoic||||||||07-NOV-08
25753|Warrow Quartzite|42738|5|Briefly described|map legend|Paleoproterozoic||||||||07-NOV-08
25753|Warrow Quartzite|43052|4|Described|p54|||of Hutchison Group||||||
25753|Warrow Quartzite|43053|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Micaceous, feldspathic quartzite.||||||07-NOV-08
25753|Warrow Quartzite|43258|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
25753|Warrow Quartzite|43298|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
25753|Warrow Quartzite|44660|14|Not recorded|map legend||Paleoproterozoic|L.Proterozoic, lithology.||||||07-NOV-08
25753|Warrow Quartzite|50605|5|Briefly described|p3.3|||Of the Hutchison Group. Geological Province: Gawler Craton & Curnamona Province.||||||
25753|Warrow Quartzite|60953|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Hutchison Group. Quartzite, pelitic schist, minor conglomerate and calcsilicate.||||||07-NOV-08
25753|Warrow Quartzite|61070|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Hutchison Group. Fine to medium-grained, flaggy, well-foliated quartzite, with feldspar and minor muscovite. Pelitic schist interbeds are common. Overlies: Kiana Granite. Geological Province: Gawler Craton.||||||12-JAN-10
25753|Warrow Quartzite|61108|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|Quartzite, pelitic schist and minor conglomerate and calcsilicate.||||||07-NOV-08
25753|Warrow Quartzite|61307|5|Briefly described|p37, p48|||Of Hutchison Gp. Partially conglomeratic feldspathic unit. Unconformably overlies Miltalie Gneiss basement below. Geological Province: Gawler Craton. See also p51 (field locality) and p68.||||||27-MAY-08
25753|Warrow Quartzite|61725|5|Briefly described|p894|Paleoproterozoic|Paleoproterozoic|Of the Hutchison Group.||||||07-NOV-08
25753|Warrow Quartzite|62893|4|Described|Map Legend, p. 4, 10, 13-14, 30,36,38-39|Early Proterozoic|Early Proterozoic|Basal unit of the Hutchison Group; unconformably overlies Archean basement. Quartz-pebble beds (highly deformed) and trough cross-bedding are common at Caralue Bluff. Probably represents an arkosic sand sequence, grading from fluvial in the west to marginal-marine in the east. Historically used for railway ballast.||Hutchison Group||Overlain by Katunga Dolomite and Lower Middleback Jaspilite.|Massive to flaggy, feldspathic and sericitic quartzite which grades from massive and muscovite-feldspar rich at the base to flaggy, coarse-grained and pelitic near the top.|
25753|Warrow Quartzite|63866|5|Briefly described|p5, p19|Orosirian|Orosirian|Cleve Domain.|c. 1900-1860 Ma|Hutchison Group||Overlain by the Middleback Subgroup.||
25753|Warrow Quartzite|65221|5|Briefly described|p28 Fig.3a |Palaeoproterozoic|Palaeoproterozoic|of Hutchison Group||||||
25753|Warrow Quartzite|65376|4|Described|p17, pp55-59. |Paleoproterozoic|Paleoproterozoic|Fluvial to marginal marine sedimentation. Contains detrital zircons from Miltalie Gneiss and Hall Bay Volcanics.|Max. deposition  2510 +/- 5 Ma to 2007 +/- 9 Ma.|Basal unit in Hutchison Group.||Locally overlies Kiana Granite.|Clean sands and local conglomerate horizons.|
25753|Warrow Quartzite|65379|5|Briefly described|p641, p642, p643, p644|Paleoproterozoic|Paleoproterozoic|Of Hutchison Group. Dolomitic marble, banded calcsilicate gneiss, minor cherty quartzite. N.B. Asbestos deposit host, contains Miltalie and Minbrie asbestos mines.||||||07-MAR-12
25753|Warrow Quartzite|65390|5|Briefly described|p17|Paleoproterozoic|Paleoproterozoic|Basal quartzite sequence of Hutchison Group.||||||
25753|Warrow Quartzite|65922|5|Briefly described|p12, p14 Tb.1, p15, p37 Fig.7|||Basal unit in Hutchison Group. Is overlain conformably by Katunga Dolomite (Middleback Subgroup); intruded by Lincoln Complex granitoids. Massive to flaggy, variably foliated micaceous and feldspathic quartzite, possibly over 1000 m thick. Forms steep NNW-trending ridges.||||||20-MAR-15
25753|Warrow Quartzite|66302|6|Mentioned|p24, p25, p33|Orosirian|Orosirian|Cleve Domain, Gawler Craton. Maximum depositional age from SHRIMP done by Fraser and Neumann (2010).|2019 +/- 3 Ma to 2003 +/- 4 Ma |Hutchison Group||Overlain by the Cook Gap Schist.||
25753|Warrow Quartzite|66882|4|Described|p101, p103 Fig.3a,c, p105-107, p109-116|Orosirian|Orosirian|Lincoln-Cleve uplands. Isotope data. Geochemistry discussed. Zircon peaks suggest derivation from underlying basement.|Max deposition 2005+/-12 Ma|Basal Darke Peak Group.||Underlies Poolalalie Dolomite. Unconformably overlies Sleaford Complex and Miltalie Gneiss.|Quartz rich sandstone.|
25753|Warrow Quartzite|67323|5|Briefly described|p29 Fig.4.1, p30|||See also Eastern Australia Time-Space Plot. Szpunar et al. (2007). Gawler Craton. Passive margin sediments and associated volcanic successions. Shown in a diagram of 1870-1820 Ma tectonics.|~1865 Ma (maximum depositional age).|Hutchison Group.||||
25753|Warrow Quartzite|67721|6|Mentioned|p33 Fig.2|||||||||
25753|Warrow Quartzite|68131|5|Briefly described|p57-58|Paleoproterozoic|Paleoproterozoic|Eastern Eyre Peninsula. ||Basal Hutchison Group.|||Clean sandstone with local conglomerate horizons.|
25753|Warrow Quartzite|68158|5|Briefly described|p4|||||Hutchison Group.|||Coarse recrystallised glassy quartzite and quartz-sericite schists.|
25753|Warrow Quartzite|69591|6|Mentioned|p105 Fig.2.98|||Appears in a diagram of the geodynamic setting of ~1790-1760 Ma eastern Australia.||||||
25753|Warrow Quartzite|69666|6|Mentioned|p27 Fig.3|Paleoproterozoic|Paleoproterozoic|||||||
25753|Warrow Quartzite|71129|5|Briefly described|p18|Paleoproterozoic|Paleoproterozoic|Geological Province: Cleve-Coulta Domain, Gawler Craton. |>2000 Ma|||||
25753|Warrow Quartzite|71235|6|Mentioned|p9|||||Hutchison Group||||
25753|Warrow Quartzite|71317|5|Briefly described|p16||Palaeoproterozoic|Cleve-Coulta Domains, Gawler Craton.|<2000 Ma|||||
25753|Warrow Quartzite|71322|6|Mentioned|p103|Paleoproterozoic|Paleoproterozoic|Northern Eyre Peninsula.||||||
25753|Warrow Quartzite|71413|5|Briefly described|p32, 33, 36, 37|Orosirian|Orosirian|Geological province: Gawler Craton. |~2005 Ma|||Intruded by Samphire granite.||
25753|Warrow Quartzite|71418|5|Briefly described|p21,24,25|Paleoproterozoic|Paleoproterozoic|Geological province: Gawler Craton. 40Ar/39Ar dating of muscovite from schists include ages of 1681+\-6, 1679+\-5  and 1674+\-6 Ma, interpreted to be post-metamorphic cooling ages (post-Kimban Orogeny).||||||
25753|Warrow Quartzite|71536|5|Briefly described|p79|||Wilgerup sequence. Outcropping in Tooligie Hill.|||||Blocky feldspathic and micaceous quartzite.|
25753|Warrow Quartzite|71859|5|Briefly described|p4, p18|Paleoproterozoic|Paleoproterozoic|Cleve and Coulta domains, southern Gawler Craton.|<2000 Ma|Hutchison Group||||
25753|Warrow Quartzite|71862|6|Mentioned|p11, p60|||||||Intruded by the Middle Camp Granite.||
25753|Warrow Quartzite|72058|5|Briefly described|p172|||Middleback Ranges, Gawler Craton.||Said to be part of Middleback Group p172, but not shown in Fig p171.||said to be overlain by the Katunga Dolomite conformably/gradationally.||18-APR-23
25753|Warrow Quartzite|72090|6|Mentioned|p10|Orosirian|Orosirian|Cleve-Coulta Domain, Gawler Craton.|<2000 Ma|||||
25753|Warrow Quartzite|72464|5|Briefly described|p1-4, 6, 9-11, 14, 28|Paleoproterozoic|Paleoproterozoic|Nankivel Dam area, Gawler Craton. Samples of schists produced post-metamorphic cooling ages of c.1681-1679 Ma (post-Kimban Orogeny).|||||Quartz-mucovite schists and muscovite-bearing quartzite. Occasional but widespread tourmaline.|
25753|Warrow Quartzite|72484|5|Briefly described|p2|||||Middleback Subgroup.||Is overlain gradationally by Katunga Dolomite.||
25753|Warrow Quartzite|73026|6|Mentioned|p7|Paleoproterozoic|Paleoproterozoic|Southern Eyre Peninsula. Overlain by unnamed metamorphosed dolomitic and pelitic units and iron formations.|c. 2000 Ma|||Unconformably overlies the Kiana Granite.||
25753|Warrow Quartzite|73027|6|Mentioned|p7|Orosirian|Orosirian||c. 2000 Ma|||Overlies the Kiana Granite.||
25753|Warrow Quartzite|73103|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic||||||Quartzite, massive, rarely cross-bedded, conglomeratic; pelitic; gneiss; nephrite.|
25753|Warrow Quartzite|73104|6|Mentioned|p3, p54|Palaeoproterozoic|Palaeoproterozoic|Geochron is a maximum depositional age. Base is locally intruded by granitic rocks.|c. 2000 Ma||||Includes medium-grained and generally well sorted quartzite with local metre-scale granular to pebbly beds.|
25753|Warrow Quartzite|73110|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic||||||Quartzite, massive, rarely cross-bedded, conglomeratic, pelitic; gneiss; nephrite.|
25753|Warrow Quartzite|73122|6|Mentioned|p32, 35, 43|||||Basal Hutchison Supergroup.||Is overlain by Katunga Dolomite.||
25753|Warrow Quartzite|73525|5|Briefly described|p19 Fig.13|Orosirian|Orosirian|Cleve Domain.|2007+/-9 Ma|Darke Peak Group|||Siliciclastics.|
27606|Watervale Sandstone Member|22889|5|Briefly described|p35|Adelaidean|Adelaidean|Parent - Saddleworth Formation. Superseds the former Watervale Sandstone as the unit is downgraded from formation to member status, see p35 for details.||||||
27606|Watervale Sandstone Member|30801|6|Mentioned|p5|||Table P5-6||||||
27606|Watervale Sandstone Member|30802|6|Mentioned|p7|||||||||
27606|Watervale Sandstone Member|30807|6|Mentioned|p103|||Suggested map symbol||||||
27606|Watervale Sandstone Member|34536|6|Mentioned|Map legend|Adelaidean|Adelaidean|Torrensian||||||
27606|Watervale Sandstone Member|37461|6|Mentioned|Table 5.I|||||||||
27606|Watervale Sandstone Member|38157|6|Mentioned|Table III|||||||||
27606|Watervale Sandstone Member|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Torrensian||||||
27606|Watervale Sandstone Member|40294|6|Mentioned|p32|||||||||
27606|Watervale Sandstone Member|41404|3|Fully described|p113|||||||||
27606|Watervale Sandstone Member|42098|6|Mentioned|p53|||||||||
27606|Watervale Sandstone Member|42222|6|Mentioned|p14|||||||||
27606|Watervale Sandstone Member|43052|5|Briefly described|p181,Table 6.1|||of Auburn Dolomite||||||
27606|Watervale Sandstone Member|44659|5|Briefly described|map legend|||Torrensian, lithology.||||||
27606|Watervale Sandstone Member|44690|4|Described|map legend|||Geol. Atlas Series. (I/54-5). Torrensian.||||||
27606|Watervale Sandstone Member|70405|6|Mentioned|p51 table 4|Neoproterozoic|Neoproterozoic|||Saddleworth Formation||||
27606|Watervale Sandstone Member|71237|14|Not recorded|p9, 19|||||||||
27606|Watervale Sandstone Member|71240|14|Not recorded|p6-7, p9, p19|||||Of Auburn Dolomite.||||
25607|Wattle Park Member|22889|6|Mentioned|Table 1 on p32|Adelaidean|Adelaidean|Parent - Stonyfell Quartzite of the Bungarider Subgroup.||||||
25607|Wattle Park Member|36835|6|Mentioned|p31|||||||||
25607|Wattle Park Member|41404|6|Mentioned|p108|||||||||
25607|Wattle Park Member|43052|5|Briefly described|p181,Table 6.1|||of Stonyfell Quartzite||||||
25607|Wattle Park Member|73188|6|Mentioned|p328|Neoproterozoic|Neoproterozoic|||Stonyfell Quartzite, Bungarider Subgroup, Burra Group||Overlain by Slapes Gully Member.||
29126|Wattleowie Granite|22631|6|Mentioned|p176|Calymmian|Calymmian|||||||
29126|Wattleowie Granite|23394|5|Briefly described|Map legend|Proterozoic|Proterozoic|||||||
29126|Wattleowie Granite|23411|6|Mentioned|Map Legend|||||||||
29126|Wattleowie Granite|23775|6|Mentioned|p728|||||||||22-SEP-09
29126|Wattleowie Granite|23818|6|Mentioned|p37|||||||||
29126|Wattleowie Granite|24197|5|Briefly described|p75 Tb. 8.1|Mesoproterozoic|Mesoproterozoic|Age: 1560Ma.||||||07-FEB-11
29126|Wattleowie Granite|30177|2|Defined|p125|Carpentarian|Carpentarian|See also p41. Prob. Carpentarian. Type locality: 4.4 miles northwest of Moolawatana Homestead, lat. 29degrees52'57"S long. 139degrees41'01"E.||||||08-DEC-22
29126|Wattleowie Granite|30807|6|Mentioned|p103|||Suggested map symbol||||||
29126|Wattleowie Granite|30920|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
29126|Wattleowie Granite|34537|6|Mentioned|p37|||||||||
29126|Wattleowie Granite|42624|4|Described|p23|||||||||
29126|Wattleowie Granite|43052|5|Briefly described|p153|||||||||
29126|Wattleowie Granite|50605|5|Briefly described|p(iii), 1.4, 10.2, Table 1.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Gawler Craton & Curnamona Province. Of the Babbage supersuite, Moolawatana Suite.||||||30-AUG-04
29126|Wattleowie Granite|62962|6|Mentioned|p2284 Fig. 2|Mesoproterozoic|Mesoproterozoic|Geological Province: Mount Painter Province.||||||07-FEB-11
29126|Wattleowie Granite|66302|6|Mentioned|p50, p78|Calymmian|Calymmian|Moolawatana Domain, Curnamona Province.|1563 +/- 3 Ma (Fraser and Neumann, 2010)|Moolawatana Suite||||
29126|Wattleowie Granite|68068|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Curnamona Province. Locally  texture can be gradational with medium-grained varieties of the younger Terrapinna Granite; intimate apophyses of the two are mapped separately. Relative age: post-Yerila Granite (i.e. c.1558 Ma) and pre-Terrapinna Granite (c.1556 Ma).|c.1557 Ma.|Unit in Moolawatana Suite.|||Weakly gneissic, white to grey adamellite, medium- to coarse-grained, minor melanocratic and minor phenocrystic varieties; composed of microcline, quartz, oligoclase, albite and biotite with accessory zircon, apatite and opaques.|
29126|Wattleowie Granite|69019|3|Fully described|p16, p23-26.|Calymmian|Calymmian|Of Coats and Blissett (1971). Enclaves, keels and roof pendants occur within Terrapinna Granite, which has very similar geochemistry. Geochemistry is detailed. Middle level intrusion. Has potential for dimension stone extraction.|c.1565-1555 Ma (U-Pb zircon; Neumann et al. 2009)|Unit in Moolawatana Suite.||Intrudes Radium Creek Group. Intruded by Mudnawatana Tonalite dykes.|Weakly gneissic, white to grey quartz monzonite; medium to coarse grained; locally melanocratic or porphyritic.|
29126|Wattleowie Granite|69023|4|Described|p17, p23-27, p37, p39-40, p42-45, p53-54|||See also p64, p76, p145, p162, p189. Coats and Blissett (1971). Mount Babbage and Mount Painter Inliers. Middle level emplacement. Geochemistry detailed. Major and trace element abundances are similar to Mount Neill Granite. Xenoliths are included in Terrapinna Granite: possibly the two granites are comagmatic. Includes xenoliths of Yerila Granite. Maximum crystallisation age. Dark grey variant has potential as dimension stone.|~1565-1555 Ma U-Pb zircon (Neumann et al., 2009).|Unit in Moolawatana Suite.||Intrudes Brindana Schist and Yerila Granite. Is intruded by Terrapinna Granite and Mudnawatana Tonalite.|Leucocratic, coarse-grained granite; pervasive gneissic overprint; metasedimentary and granitic xenoliths widespread.|
29126|Wattleowie Granite|69562|5|Briefly described|p670 Tb.5|||Magmatic crysalisation age.|1563 +/- 3 Ma (Fraser and Neumann, 2010).||||Biotite granite with biotite foliation.|06-APR-22
29126|Wattleowie Granite|69650|5|Briefly described|p62|Calymmian|Calymmian|Suggested to come from the same magma source as Coulthard Suite and Pepegoona Porphyry.|~1560 Ma.|Unit in Moolawatana Suite.||||
29126|Wattleowie Granite|70384|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Mineralogy: microcline, quartz, oligoclase, albite, biotite; accessory zircon, apatite, opaques. The same age was determined by SHRIMP and ICPMS.|1563 +/- 3 Ma (U-Pb zircon).|||Is intruded by Terrapinna Granite.|Weakly gneissic, white to grey quartz monzonite, medium- to coarse-grained, minor melanocratic and porphyritic forms. Locally gradational with medium-grained Terrapinna Granite and has associated apophyses (part deformed).|
29126|Wattleowie Granite|71531|14|Not recorded|p10||Carpentarian|||||||
29126|Wattleowie Granite|72456|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Marree 1:250k map sheet. |||||Granite, grey-white, leucocratic, weakly gneissic.|
29126|Wattleowie Granite|73061|4|Described|p1067, p1069, p1071-1072, p1076-1077|Calymmian|Calymmian|Mount Painter Province. High heat producing granite. Gradational contact with Terrapinna Granite suggests it to be comagmatic. SHRIMP U-Pb zircon crystallisation age 1563 +/- 3 Ma (Fraser and Neumann, 2010). Mean eHf value of +1.1 +/- 1.1. Associated with mafic magmatism, crosscut by a mafic dyke (1565 +/- 10 Ma crystallisation age). Contains inherited zircons. Location in text includes p1068 Fig.1, p1070 Tb.1, p1074.|1562 +/- 26 Ma U-Pb LA-ICPMS, 1557 +/- 6 Ma|||Intrudes the Terrapinna Granite.|Includes fine-grained, pale grey to white equigranular granite.|
79322|Waukaloo Member|70405|4|Described|p23|Paleoproterozoic|Paleoproterozoic|||Peryhumuck Formation||Overlies and interfingers Peryhumuck Formation|Schistose, fine grained psammite and metasiltstone.|
26205|Waurea Pyroclastics|24474|4|Described|p41|Mesoproterozoic|Mesoproterozoic|Of the Glyde Hill Volcanic Complex.  Lapilli-tuff to tuff breccia overlain by Wheepool Rhyolite as interpreted by Giles; but included within the Wheepool Rhyolite by Blissett (1980).  Geological Province: Gawler Craton.||||||
26205|Waurea Pyroclastics|30984|2|Defined|p12|Proterozoic|Proterozoic|||||||
26205|Waurea Pyroclastics|41974|5|Briefly described|Table 1 P412|||||||||
26205|Waurea Pyroclastics|43052|5|Briefly described|p111|||||||||
26205|Waurea Pyroclastics|43094|5|Briefly described|p26|||||||||
26205|Waurea Pyroclastics|67909|5|Briefly described|p126-127, 129, 132-134, 139|Mesoproterozoic|Mesoproterozoic|Lake Everard area. Contains well-preserved quartz-phenocryst-hosted melt inclusions (experiments detailed).||Glyde Hill Volcanic Complex.|||Contains several different pyroclastic facies, including poorly-sorted crystal tuff.|
26205|Waurea Pyroclastics|70659|5|Briefly described|p7-8|Mesoproterozoic|Mesoproterozoic|Over 3m thick.||Glyde Hill Volcanic Complex.|||Laminated, moderately sorted volcaniclastic deposit containing feldspar and quartz crystals with minor pumice; low angle truncations, scours and cross-beds.|
26205|Waurea Pyroclastics|70816|5|Briefly described|p5|||Lake Everard area, Gawler Ranges.||Unit of Glyde Hill Volcanic Complex.||Overlain by Bunburn Dacite. Underlain by Wheepool Rhyolite.||
26205|Waurea Pyroclastics|72090|6|Mentioned|p12|||Gawler Craton.||Glyde Hill Volcanic Complex||||
79114|Weena sandstone|69982|5|Briefly described|p17-19, p42, p61, p110, p166, p220|Devonian|Cambrian|Warburton Basin. Informal name for a unit in the interval 1632.0 - 1644.1 m in the Weena 1 well. Also appears as Weena Sandstone (p110, p166). Age unknown. Composite log shown. Bedding dip angles in wells listed.|||||Unique red-brownish, moderately to poorly sorted, very coarse to granule size quartzarenite interbedded with medium sandstone and minor mudstone; numerous vertical Skolithos burrows.|28-AUG-15
39164|Weetulta Formation|24475|2|Defined|p53|Paleoproterozoic|Paleoproterozoic|Of Wallaroo Group. Interfingers with Wandearah Formation.||||||07-NOV-08
39164|Weetulta Formation|60958|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Wallaroo Group. Felsic volcanics and intrusives. Intruding or interlayered with metasediments. Geological Province: Gawler Craton.||||||07-NOV-08
39164|Weetulta Formation|61121|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|All felsic volcanics and intrusives in the Wallaroo Group. Intruding or interlayered with metasediments.  Age: ~1800Ma.Geological Province: Gawler Craton.||||||09-JUL-13
39164|Weetulta Formation|65375|5|Briefly described|p19, p22.|||Encompasses all felsic volcanics in the Wallaroo Group. Ranges from syndepositional extrusive to shallow intrusive volcanics.|1741-1736 Ma.|Unit in Wallaroo Group.|Comprises Moonta Porphyry Member, Wardang Volcanics Member and Mona Volcanics Member.|||
39164|Weetulta Formation|65376|5|Briefly described|pp101-111. |||||Unit in Wallaroo Group.|Includes Moonta Porphyry Member, Wardang Volcanics Member and Mona Volcanics Member.|||
39164|Weetulta Formation|66302|5|Briefly described|p29, p33|Statherian|Statherian|Olympic Domain, Gawler Craton. Age derived from U-Pb dating of its constituent members. ||Wallaroo Group|Includes the Moonta Porphyry Member, Mona Volcanics Member, Wardang Volcanics Member and the Doora Member.||A-type felsic volcanic rocks.|
39164|Weetulta Formation|67181|5|Briefly described|p629|Statherian|Statherian|From the south-eastern Gawler Craton, volcanic members age of ca 1770-1750 Ma from Fanning et al. (2007)|ca 1770-1750 Ma|Unit in Wallaroo Group|Includes Wardang Volcanics Member, Moonta Porphyry Member|||
39164|Weetulta Formation|67536|5|Briefly described|Map Legend|Statherian|Statherian|Gawler Craton.|1765 +/- 27 Ma - 1741 +/- 7 Ma|Of the Wallaroo Group.|||Felsic metavolcanic rocks.|
39164|Weetulta Formation|69748|6|Mentioned|p179-180|Paleoproterozoic|Paleoproterozoic|Moonta-Wallaroo region, Olympic IOGC Province.||Wallaroo Group.|Moonta Porphyry, Wardang Volcanic, Members.|||
39164|Weetulta Formation|70382|6|Mentioned|p33|||||Unit of Wallaroo Group.|Includes Doora Member.|||
39164|Weetulta Formation|71129|6|Mentioned|p39|Statherian|Statherian|Geological Province: Gawler Craton. Deposition synchronous with Wandearah Formation.||||||
39164|Weetulta Formation|73026|5|Briefly described|p9|Paleoproterozoic|Paleoproterozoic||||||Acid volcanics.|
39164|Weetulta Formation|73027|5|Briefly described|p9,|Palaeoproterozoic|Palaeoproterozoic||||||Acid volcanics.|
39164|Weetulta Formation|73092|6|Mentioned|p2|Paleoproterozoic|Paleoproterozoic|||||||
39164|Weetulta Formation|73103|5|Briefly described|Map legend.|||Is shown in the Solid Geology Interpretation map, below the main Whyalla 250k map.||||||
24094|Wertigo Granite|22834|6|Mentioned|P39|||||||||
24094|Wertigo Granite|23719|4|Described|p19|Statherian|Orosirian|Age: 1828+/-34 Ma (U-Pb zircon). See also page 15 Table 2, page 19 Table 5. Of Lincoln Complex. Geological Province: Gawler Craton.||||||
24094|Wertigo Granite|24197|5|Briefly described|p74 Tb. 8.1|Paleoproterozoic|Paleoproterozoic|Age: 1750-1700Ma.||||||07-FEB-11
24094|Wertigo Granite|39349|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
24094|Wertigo Granite|40448|6|Mentioned|p34|||||||||
24094|Wertigo Granite|40644|6|Mentioned|p133|||Previously "Tor Granite" of Miles (1954). Age: 1760Ma (Rb-Sr whole rock; Compston et al 1966).||||||13-AUG-08
24094|Wertigo Granite|41667|6|Mentioned|p12|||||||||
24094|Wertigo Granite|41972|6|Mentioned|Fig.5 P375|||||||||
24094|Wertigo Granite|42934|5|Briefly described|p520 Fig.1|||||||||
24094|Wertigo Granite|43052|5|Briefly described|Table 4.4|||Of Moody Suite.||||||05-MAR-08
24094|Wertigo Granite|50605|5|Briefly described|p(i), 1.3, 5.2, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Gawler Craton and Curnamona Province. Of the Moody Suite (Younger Lincoln Supersuite).||||||02-JUN-09
24094|Wertigo Granite|60953|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Lincoln Complex. Granite, granodiorite.||||||07-NOV-08
24094|Wertigo Granite|61108|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|Granite and granodiorite.||||||07-NOV-08
24094|Wertigo Granite|65376|5|Briefly described|p39, pp72-73.|Paleoproterozoic|Paleoproterozoic|Revised geochronology indicates this unit is not part of the Moody Suite, nor does it intrude the Myola Volcanics.|1845 +/- 21 Ma.||||Medium-grained foliated granite to granodiorite gneiss.|
24094|Wertigo Granite|65922|6|Mentioned|p31|Statherian|Statherian|Interpreted age of ~1745-1710 Ma. Probable equivalent to some Lincoln Complex granitoids.||||||
24094|Wertigo Granite|66302|6|Mentioned|p28|||Igneous crystallisation ages. |1792 +/- 6 and 1768 +/- 4 Ma (SHRIMP U-Pb)|||Intrudes the Myola Volcanics.||
24094|Wertigo Granite|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Southern Gawler Craton. Two intrusions are shown on the Time-Space Plot.|1755 +/- 19 Ma and 1768 +/- 4 Ma.|||||
24094|Wertigo Granite|68158|5|Briefly described|p2|Proterozoic|Proterozoic|Middleback Range.|1845 +/- 21 Ma (Fanning et al., 2007).|||||
24094|Wertigo Granite|70027|6|Mentioned|p71|Statherian|Statherian|Geological province: Gawler Craton. Possible source of ca. 1790-1750 Ma zircons associated with the Warramboo magnetite gneiss.|ca. 1790 Ma|||||
24094|Wertigo Granite|70659|6|Mentioned|p4|Palaeoproterozoic|Palaeoproterozoic|Kimban Orogeny (1730-1690 Ma) tectonic fabrics were folded by (~1620-1570 Ma) Kararan Orogeny.||||||
24094|Wertigo Granite|70721|4|Described|p63-p65, p67-p70, p72-p74|Paleoproterozoic|Paleoproterozoic|Spencer Domain, Gawler Craton. Exposed 25km southwest of Whyalla near Broadbent Hill and is an elliptical intrusion 12-14km north-south by 8-9km east-west. Petrography, deformational fabrics, geochemistry and geochronology are discussed in detail. Majority of granites are classified as peraluminous two mica granites. Granodiorites are ferroan alkal-calcic metaluminous granites.|c. 1790-1770 Ma (Fraser and Neumann, 2010)||||Medium- to coarse-grained granite to granodiorite.|
24094|Wertigo Granite|71037|5|Briefly described|p21 Fig.1|Paleoproterozoic|Paleoproterozoic|Shown only on 'Outcropping geology and mineral deposits of northern Eyre Peninsula' map p21 Fig.1.|c. 1775 Ma.|||Shown as younger than Myola Volcanics and Broadview Schist and older than Tip Top Granite.||
24094|Wertigo Granite|71129|5|Briefly described|p17,18,204|Statherian|Statherian|Geological Province: Spencer Domain, Gawler Craton. Contains metamorphic growth zircons dated at 1764+\-5 Ma (Fraser and Neumann, 2010); affected by same deformation event as the Tip Top Granite and Minbrie Gneiss.|1790-1770 Ma|||||
24094|Wertigo Granite|71317|5|Briefly described|p15-p16|Palaeoproterozoic|Palaeoproterozoic|Spencer Domain, Gawler Craton.|c. 1790-1770 Ma|||||
24094|Wertigo Granite|71318|5|Briefly described|p3,15-16|Paleoproterozoic|Paleoproterozoic|Geological province: Gawler Craton. Sample GSSA 2017961 (weakly foliated biotite-granite) yielded two zircon phases with interpreted (weighted mean 207Pb/206Pb) magmatic crystallisation ages of 1789+\-18 Ma (consistent with 1792+\-6 magmatic age of Fanning et al. (2007)), and at 1580+\-12 Ma. This second age was previously attributed to Pb loss in previous studies, however as the c. 1580 Ma zircon in this sample includes concordant and near concordant data, it is likely (and the preferred explanation) that the c. 1789 Ma and c. 1580 Ma ages may be that of leucocratic veins within the Wertigo Granite (see description in Fraser and Neumann 2010), and newly introduced granitic veins at c. 1580 Ma. Further sampling is required to better distinguish between the leucocratic veins and host granitic gneiss, and therfore test the hypothesis for the presence of 1580+\-12 Ma zircon populations.  Zircon characteristics, petrography, U-Pb isotopic results and geochronological interpretation are provided.|||||Grey, medium-grained granite with weak foliation defined by fine discontinuous strings of biotite.|10-DEC-19
24094|Wertigo Granite|71413|6|Mentioned|p32 Fig 2|||Geological province: Gawler Craton. ||||||
24094|Wertigo Granite|71559|6|Mentioned|p15 Fig 1|Paleoproterozoic|Paleoproterozoic|Geological province: Gawler Craton.||||||
24094|Wertigo Granite|71859|5|Briefly described|p1-p4, p6|Statherian|Statherian|Spencer Domain, southern Gawler Craton.|c. 1790-1770 Ma|||||
24094|Wertigo Granite|71862|6|Mentioned|p2-p3, p8, p12, p15|Statherian|Statherian|Originally a part of the now obsolete Lincoln Complex.|c. 1790-1770 Ma|||||
24094|Wertigo Granite|72058|5|Briefly described|p172|||Middleback Ranges, Gawler Craton. Intruded in association with an intracontinental rifting event dated at roughly 1790 Ma.|~1790-1770 Ma|||||
24094|Wertigo Granite|72090|6|Mentioned|p10|Statherian|Statherian|Spencer Domain, Gawler Craton.|1790-1770 Ma|||||
24094|Wertigo Granite|72459|6|Mentioned|p8, p51|Paleoproterozoic|Paleoproterozoic|Whyalla region.|ca. 1828 Ma|||||
24094|Wertigo Granite|72462|6|Mentioned|p3|Paleoproterozoic|Paleoproterozoic|Gawler Craton.||||||
24094|Wertigo Granite|72463|6|Mentioned|p2|Paleoproterozoic|Paleoproterozoic|||||||
24094|Wertigo Granite|72484|6|Mentioned|p2|||Emplaced during a continental rifting episode.|~1.79 Ga|||||
24094|Wertigo Granite|73103|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic||1792-1768 Ma (U-Pb; crystallisation).||||Granite; granodiorite, gneissic, migmatitic, pink and grey.|
24094|Wertigo Granite|73130|6|Mentioned|[poster] Fig.1|Paleoproterozoic|Paleoproterozoic|||||||28-OCT-22
24094|Wertigo Granite|73235|6|Mentioned|p53|Statherian|Statherian|Gawler Craton. Spencer region.|1790-1770 Ma|||||
24094|Wertigo Granite|73525|5|Briefly described|p19 Fig.13, p20|Statherian|Statherian|Spencer Domain. eHf values of approximately -4.|1775 Ma||||Felsic intrusive.|
30305|Western Spur Limestone|68713|5|Briefly described|p19|Early Cambrian|Early Cambrian|New name.||Of the Hawker Group.||||
30305|Western Spur Limestone|69019|2|Defined|p61, p67-69, p164-165, p229.|Early Cambrian|Early Cambrian|New name; of Sheard and Reid (2012). Formerly part of Billy Springs Formation. Type area 2.2 km SE of Pelican Well and 5.5 km WSW of Mount Freeling Homestead; thickness to ~200 m. Considered a distal equivalent of Parachilna Formation or Woodendinna Dolomite to the S. Recently (2011) associated with Fe-Mn mineralisation near Western Spur.||Unit in Hawker Group.||Disconformably overlies Uratanna Formation.|Light to dark grey fine-grained ooid grainstone, massive to bedded and cross-bedded; buff-coloured dolostone interbeds upsection contain rare stromatolites and ?recrystallised archaeocyaths.|
30305|Western Spur Limestone|70384|5|Briefly described|Map legend.|Early Cambrian|Early Cambrian|Arrowie Basin. Shallow lagoonal deposits.|||||Light to dark grey, fine-grained, massive ooid grainstone, planar-bedded to cross-bedded; buff-yellow, fine-grained crystalline dolostone as interbeds in upper section with rare stromatolites. Sharp erosional base.|
30305|Western Spur Limestone|72456|5|Briefly described|Map Legend|Cambrian|Cambrian|Marree 1:250k map sheet. |||||Ooid grainstone, light-dark grey, massive, bedded and crossbedded; dolostone, buff, fine-grained, crystalline as interbeds in upper part. Rare stromatolites, sharp erosional base.|
80218|Whaler Hut Member|73162|5|Briefly described|p452, p453, p458|Mesoproterozoic|Mesoproterozoic|Roopena Basin. Deposited in southeast part of the preserved basin. Records episode of extra-basinal felsic volcanism synchronous with sedimentation of Fresh Well Formation. Written as both Whaler Hut Member, p452, 453, and Whalers Hut Member, p458. Lower of three tuff members in the upper Fresh Well Formation. 0.5 m thick.||Fresh Well Formation, upper||Interlayered with the upper Fresh Well Formation.|Well sorted and laminated tuff, composed of quartz and minor lithic felsic volcanic and sedimentary clasts, matrix of sericite and clay, sharp basal and sharp to gradational upper contacts, approximately 0.5 m thick.|
73301|Whalers Bluff Supersequence|63134|2|Defined|112|||||||||
73301|Whalers Bluff Supersequence|63269|5|Briefly described|p605|Pleistocene|Pliocene|Otway Basin.||||Overlies Heytesbury Supersequence.||
73301|Whalers Bluff Supersequence|69297|6|Mentioned|p80, p98, p110, p111|||||||||
73301|Whalers Bluff Supersequence|69651|5|Briefly described|p10, p12-15, p17-19, p22, p29, p49-50|Pleistocene|Pliocene|Open marine deposits. Possible seals.||||Overlies Heytesbury Supersequence.|Calcareous claystone overlain by marls, calcarenite and calcilutite; shaly limestone overlain by calcarenite and calcilutite; quartz sandstone overlain by silty mudstone, and limestone.|
73301|Whalers Bluff Supersequence|70077|5|Briefly described|Regional: Fig.4; p4|Holocene|Miocene|Otway Basin.||||Overlies Heytesbury Supersequence.||
73301|Whalers Bluff Supersequence|70078|5|Briefly described|Regional: Fig.4; p3|Holocene|Neogene|||||Overlies Heytesbury Supersequence.|Shelfal marls and limestones.|
73301|Whalers Bluff Supersequence|70880|6|Mentioned|p77|Pleistocene|Pliocene|Otway Basin.||||Overlies Heytesbury Supersequence.||
73301|Whalers Bluff Supersequence|71266|5|Briefly described|p614 Fig.3, p615|Pleistocene|Pliocene|Otway Basin.||||Overlies Heytesbury Supersequence.||
27949|Whenan Member|39047|4|Described|p805|||||||||
27949|Whenan Member|39871|6|Mentioned|p1944|||||||||
27949|Whenan Member|41125|6|Mentioned|Fig.18|||||||||
27949|Whenan Member|41493|5|Briefly described|Table 2|||||||||
27949|Whenan Member|42022|6|Mentioned|p5|||||||||
79311|Whey Whey Member|70339|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|||probably of Peryhumuck Formation.|||Psammopelite.|
79311|Whey Whey Member|70405|4|Described|p23, p43 Table 3|Paleoproterozoic|Paleoproterozoic|||Peryhumuck Formation||Interfingers with Peryhumuck Formation|Schistose metasedimentary rock of pelitic to psammopelitic composition.Psammite interbedding with sedimentary structures. Pelitic Schist contains sericite pseudomorphs.|
79311|Whey Whey Member|70658|5|Briefly described|p6, 10, 15, 19, 21, 29|Paleoproterozoic|Paleoproterozoic|Olary Domain, Curnamona Province.||Peryhumuck Formation.|||Clastic metasediments: psammite and psammopelite.|
29948|White Dam Subsuite|22430|6|Mentioned|p2||Proterozoic|||||||
29948|White Dam Subsuite|43052|5|Briefly described|p128, Table 5.6|||Hiltaba Suite. Restricted to subsurface. Age: 1590 +/-10 Ma U-Pb zircon (Creaser and Cooper, 1993), but don't know what was dated.|||||Variety of rock types including quartz monzodiorite, quartz monzonite and aplite|13-SEP-12
29948|White Dam Subsuite|65390|5|Briefly described|p26 Tb. 1|Calymmian|Calymmian|Of Hiltaba Suite. Variety of rock types including quartz monzodiorite, quartz monzonite and aplite. Restricted to subsurface. Age of 1590 +/- 10 Ma (U-Pb zircon: Creaser and Cooper, 1993).||||||
29948|White Dam Subsuite|72065|6|Mentioned|p112|||Geological province: Olympic Province, Gawler Craton. Contains 'HS-type' crystal clusters: fine- to medium-grained magnetite-apatite+\-titanite+\-biotite-chlorite+\-zircon. (HS: Hiltaba Suite type).||||||
83514|White Hill Complex|73155|5|Briefly described|p271 Fig.4, p282 Fig.13, p283-284, p286|Calymmian|Calymmian|Mount Woods Domain, southern. Occurs as a distinct circular feature that may reflect folding about a relatively open synclinal structure, or conditions of emplacement. Alternating high and low layering geophysical response (reflecting lithological layering). See also p277, p279. See also White Hills Complex.|ca. 1562 Ma||||Includes pyroxenite, norite and gabbro with plagioclase and pyroxene-rich layers, interleaved disseminated to massive magnetite-ilmenite bands.|
38062|White Pointer Supersequence|24336|5|Briefly described|p99 Fig.3|||Correlated to the Platypus Formation.||||||
38062|White Pointer Supersequence|61544|6|Mentioned|p367 Fig.3. |Cenomanian|Cenomanian|Ceduna Sub-basin. Accelerated subsidence.||||Overlies Blue Whale Supersequence. Is overlain by Tiger Supersequence.||
38062|White Pointer Supersequence|66578|6|Mentioned|p1007 Fig.3.|Late Cretaceous|Late Cretaceous|Ceduna Sub-Basin, Bight Basin.||||Overlies Blue Whale Supersequence. Is overlain by Tiger Supersequence.||
38062|White Pointer Supersequence|69297|5|Briefly described|p14 fig 2.4, p23|Cenomanian|Cenomanian|Eyre, Ceduna and Duntroon Sub-basins. Deposited in marine to deltaic environments. Good faulting seal capacity for hydrocarbons and good potential oil and gas source rocks. Seismic interpretation suggests this unit contains a broad band of coaly sediments. Maximum thickness of approximately 5000m. See also p25 fig 2.9, p26 fig 2.11, p28, p37, p41-p44, p45 fig 2.17, p58, p60.||||Overlies the Blue Whale Supersequence. Overlain by the Tiger Supersequence.||
38062|White Pointer Supersequence|70067|5|Briefly described|Ceduna: Fig.2; p2. Regional: Fig.2; p2|Cenomanian|Cenomanian|Bight Basin. Consists mostly of Platypus Formation. Potential reservoir. Coals are potential source rocks.||||Overlies Blue Whale Supersequence. Is overlain by Tiger Supersequence.|Prograding deltaic sediments, including a broad band of coaly sediments.|
24632|White Well Granite|22631|6|Mentioned|p176|Calymmian|Calymmian|||||||
24632|White Well Granite|24197|5|Briefly described|p75 Tb. 8.1|Mesoproterozoic|Mesoproterozoic|Age: 1560Ma.||||||07-FEB-11
24632|White Well Granite|42624|2|Defined|p22|Mesoproterozoic|Mesoproterozoic|Reserved.||||||
24632|White Well Granite|42885|6|Mentioned|p29|||||||||
24632|White Well Granite|43052|5|Briefly described|p153|||||||||
24632|White Well Granite|50605|5|Briefly described|p(iii), 1.4, 10.2, Table 1.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Gawler Craton & Curnamona Province. Of the Moolawatana Suite (Babbage supersuite).||||||
24632|White Well Granite|68068|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Curnamona Province.||Unit in Moolawatana Suite.||Intrudes Petermorra Volcanics.|Tabular feldspar biotite granite, greyish, composed of microcline, bluish quartz, plagioclase, biotite and secondary muscovite, with accessory zircon, monazite and apatite.|
24632|White Well Granite|69019|6|Mentioned|p30 Fig.10.|Calymmian|Calymmian|Mt. Babbage Inlier.|c.1555 Ma.|||||
24632|White Well Granite|69023|4|Described|p26, p27, p35-37, p49-50, p189|||Defined Sheard et al. (1992) after informal use by Teale et al. (1989). Had been previously included in Terrapinna Granite by Coats et al. (1969). Mount Babbage Inlier. Geochemistry detailed. Age unknown, but younger than Petermorra Volcanics.||Unit in Moolawatana Suite.||Intrudes Petermorra Volcanics. Is faulted against Terrapinna Granite.|Deformed, medium-grained biotite granite, monzogranite; has aligned K-feldspar and prismatic plagioclase phenocrysts, bluish to grey quartz, decussate biotite aggregates; mica foliation from post-emplacement deformation.|
24632|White Well Granite|69562|5|Briefly described|p670 Tb.5||||1556 +/- 4 Ma (Sheard et al. 1992).||||Biotite granite.|
24632|White Well Granite|70384|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|||||Intrudes Petermorra Volcanics.|Tabular feldspar biotite granite, greyish. Composed of microcline, bluish quartz, plagioclase, biotite and secondary muscovite, with accessory zircon, monazite and apatite.|
24632|White Well Granite|72459|4|Described|p63-64, p86-89, p94-98|Mesoproterozoic|Mesoproterozoic|Together with the Wattleowie granite, Terrapinna Granite, Golden Pole granite and the Petermorra Volcanics forms sub""group"" 2b of this report. Outcrops as small plugs within the Petermorra Volcanics in the Mt Babbage inlier. Distinctive chemical features were not identified in this study.||Moolawatana Suite|||Deformed, medium-grained, equigranular granite.|
26214|Wigunda Formation|22485|4|Described|p51 , Fig 2 & p53|Late Cretaceous|Late Cretaceous|||||||
26214|Wigunda Formation|22663|5|Briefly described|S97-1 and 2 p3||Late Cretaceous|||||||
26214|Wigunda Formation|23792|5|Briefly described|Fig.D4|Santonian|Cenomanian|Equivalent to Tiger supersequence. Overlies Platypus Formation. Overlain by Potoroo Formation. Geological Province: Bight Basin.||||||15-JUN-05
26214|Wigunda Formation|24201|5|Briefly described|p373 Fig. 2|Santonian|Cenomanian|||||||
26214|Wigunda Formation|24338|5|Briefly described|p938 Fig. 2|Santonian|Cenomanian|Overlain by the Potoroo Formation. Overlies the Platypus Formation. Formation is Fm. in text. Geological Province: Bight Basin.||||||
26214|Wigunda Formation|24350|5|Briefly described|Fig. 4 Appdx|Santonian|Cenomanian|Shown as equivalent to part of White Pointer and Tiger Supersequences.||||||21-JAN-16
26214|Wigunda Formation|24443|5|Briefly described|Fig.7|Santonian|Cenomanian|Overlies Platypus Formation. Geological Province: Bight Basin.||||||
26214|Wigunda Formation|24553|5|Briefly described|p36, Figs. 7 and 10|Late Cretaceous|Late Cretaceous|Geological Province: Duntroon Sub-basin. Significant oil shows. Contains pro-delta claystones. Appears as part of both Tiger and Hammerhead Supersequences.||||||07-FEB-11
26214|Wigunda Formation|34759|6|Mentioned|Fig.7|||Stratigraphy||||||
26214|Wigunda Formation|38221|6|Mentioned|Fig.4|||Great Australian Bight Basin||||||
26214|Wigunda Formation|41751|6|Mentioned|p3|||||||||
26214|Wigunda Formation|42075|5|Briefly described|Fig.10 P250|||||||||
26214|Wigunda Formation|42545|2|Defined|p9|Campanian|Turonian|||||||
26214|Wigunda Formation|43026|5|Briefly described|Table 1,p586|||||||||
26214|Wigunda Formation|43814|6|Mentioned|Fig.3,p115|||||||||
26214|Wigunda Formation|44133|5|Briefly described|p137, 141|Campanian|Turonian|Maximum Thickness: 665m. Correlative of Belfast Mudstone. Includes Wombat Sandstone Member.||||||
26214|Wigunda Formation|44145|6|Mentioned|p554|||From Ceduna Terrace. Probably equivalent age to Nurina Formation, Eucla Basin (and therefore Late Cretaceous).||||||
26214|Wigunda Formation|61544|6|Mentioned|p367 Fig.3. |Campanian|Cenomanian|||||Overlies Platypus Formation. Is overlain by Potoroo Formation.||
26214|Wigunda Formation|61630|6|Mentioned|p554, p555 Fig. 3, p556, p557, p559|Paleocene|Late Cretaceous|Geological Province: Bright and Duntroon Basins.||||||07-APR-09
26214|Wigunda Formation|63125|6|Mentioned|p122|||Geological Province: Duntroon Basin||||||
26214|Wigunda Formation|69297|5|Briefly described|p14 fig 2.4, p25 fig 2.9|Campanian|Turonian|Ceduna and Duntroon Sub-basins. Deposited in a dominantly marine environment, with the exception of shales and mudstones which were deposited under prodelta conditions. Good reservoir and seal potential. See also p39 fig 2.14, p58, p60, p64.|||Includes the Wombat Sandstone Member.|Overlies the Platypus Formation. Overlain by the Potoroo Formation.|Shale and mudstone.|
26214|Wigunda Formation|70067|5|Briefly described|Ceduna: Fig.2; p1. Regional: Fig.2|Campanian|Cenomanian|Bight Basin. Minor gas shows and oil indications were encountered in Greenly 1.|||Wombat Sandstone Member.|Overlies Platypus Formation. Is overlain by Potoroo Formation.||
35691|Wilari Dolomite Member|23282|2|Defined|p62||Neoproterozoic|of Sukanata (1993) and formally defined by Zang (1995). Age: Precambrian, Neoproterozoic, mid-Marinoan.||||||
35691|Wilari Dolomite Member|24112|5|Briefly described|p254 Fig.2|Neoproterozoic|Neoproterozoic|Of the Ungoolya Group. Geological Province: Officer Basin||||||
35691|Wilari Dolomite Member|50127|6|Mentioned|p48 Fig.2|||Geological Province: Officer Basin||||||
35691|Wilari Dolomite Member|61732|5|Briefly described|p63, p99|||Of the Tanana Formation (Ungoolya Group). See also p123, p128, p145 Fig. 51.||||||07-FEB-11
35691|Wilari Dolomite Member|63397|2|Defined|31|Neoproterozoic III|Neoproterozoic III|Of the Tanana Formation. Type section in text. Dolomite, probably secondary. Max Thickness: 61m. Overlies: Karlaya Limestone Member unconformably.||||||18-JUL-07
35691|Wilari Dolomite Member|63811|6|Mentioned|p505, Fig 2, p521|||||Of Ungoolya Group.||||28-MAR-12
35691|Wilari Dolomite Member|67912|5|Briefly described|p13-14|Ediacaran|Ediacaran|Eastern Officer Basin. Subsurface; penetrated by the Lake Maurice West 1 drillhole.||Tanana Formation.||Overlies Karlaya Limestone. Is overlain by Observatory Hill Formation.||
35691|Wilari Dolomite Member|72478|6|Mentioned|p8|Marinoan|Marinoan|Officer Basin.|c. 585 Ma|Tanana Formation||||24-MAR-21
35691|Wilari Dolomite Member|73099|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Officer Basin.||Tanana Formation.||Overlies Karlaya Limestone. Is overlain by Narana Formation.|Pale to dark grey, vuggy, stylolitic dolostone and dolomitic limestone.|
68798|Wilcolo Sandstone Member|60418|5|Briefly described|p134 Fig.1|Neoproterozoic|Neoproterozoic|Of Bunyeroo Formation.||||||
68798|Wilcolo Sandstone Member|60959|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Of the Bunyeroo Formation. Thin pebbly lag sandstone or massive coarse grained to pebbly, cross bedded channelised sandstone. Fluvial to shallow marine.||||||
68798|Wilcolo Sandstone Member|61732|5|Briefly described|p28 Fig. 13|Marinoan|Marinoan|Of the Bunyeroo Formation (Wilpena Group).  Geological Province: Adelaide Rift Complex.||||||07-FEB-11
68798|Wilcolo Sandstone Member|62784|5|Briefly described|p8 Fig.1|Neoproterozoic|Neoproterozoic|Top of Bunyeroo Formation, Wilpena Group. Overlain by Wonoka Formation.||||||
68798|Wilcolo Sandstone Member|64455|5|Briefly described|p138 Fig.1|Ediacaran|Ediacaran|Of Bunyeroo Formation.||||||29-JAN-09
68798|Wilcolo Sandstone Member|68030|5|Briefly described|p238|Ediacaran|Ediacaran|Flinders Ranges. Basal lowstand sequence infilling local incisions into the top of ABC Range Quartzite.||Unit of Bunyeroo Formation.||Underlain/infills into ABC Range Quartzite.|Lowstand veneer of conglomerate and pebbly sandstone.|
29767|Wildildie Sandstone Member|22510|5|Briefly described|p39, table1|||Age: Marinoan||||||
80436|Wilgerup schist|71536|5|Briefly described|p4, p79-p80, p83, p211|Paleoproterozoic|Archean|Age is a SHRIMP U-Pb date derived from this publication. Maximum depositional age (from 3 grains): 1864+/-12 Ma. Provenance ages: 2447 +/- 6 Ma, 2519 +/- 5 Ma.|1864+/-12 Ma U/Pb zircon SHRIMP|Hutchison Group|||Siliceous iron formation.|03-APR-18
25626|Willalinchina Sandstone|22929|6|Mentioned|27|||Underlying unit Watchie Sandstone||||||
25626|Willalinchina Sandstone|24175|3|Fully described|p35, p32 Fig. 6|Middle Eocene|Middle Eocene|Previously included in the Watchie Sandstone under which it appears to lens out.  Max. thickness: 10m.  Geological Province: Billa Kalina Basin.||||||
25626|Willalinchina Sandstone|24321|5|Briefly described|Map legend|Early Eocene|Late Paleocene|Geological Province: Billa Kalina Basin||||||
25626|Willalinchina Sandstone|42340|6|Mentioned|p25|||Described in 1986, Ref 91/27299.||||||
25626|Willalinchina Sandstone|42375|4|Described|p84, p89|||Billa Kalina Basin. See also P30, 32. See also Willalinchina Formation P79.Age Eocene? to Oligocene?||||||
25626|Willalinchina Sandstone|42465|5|Briefly described|Map Legend|||||||||
25626|Willalinchina Sandstone|42469|6|Mentioned|p39|||||||||
25626|Willalinchina Sandstone|43052|5|Briefly described|Table 2.1|||||||||
25626|Willalinchina Sandstone|43053|5|Briefly described|Map Legend|Eocene|Paleocene|Fluvial sand. Geological Province: Billa Kalina Basin.||||||25-MAY-05
25626|Willalinchina Sandstone|43258|5|Briefly described|Map Legend|Eocene|Paleocene|||||||
25626|Willalinchina Sandstone|43298|5|Briefly described|Map Legend|Eocene|Paleocene|||||||
25626|Willalinchina Sandstone|44133|5|Briefly described|p195, 190 Fig. 10.30|Early Pliocene|Middle Eocene|Geological Province: Billa Kalina Basin. ||||||
25626|Willalinchina Sandstone|60953|5|Briefly described|Map Legend|Pliocene|Miocene|Fluviolacustrine sand, often silcreted. Geological Province: Billa Kalina Basin.||||||
25626|Willalinchina Sandstone|61108|5|Briefly described|map legend|Pliocene|Miocene|Fluviolacustrine sand, often silcreted. Geological Province: Billa Kalina Basin.||||||31-MAY-05
25626|Willalinchina Sandstone|61155|5|Briefly described|p17|Middle Eocene|Middle Eocene|Age: ~48.5-~42Ma. Geological region: Billa Kalina area.||||||
25626|Willalinchina Sandstone|65194|6|Mentioned|p49|Miocene|Oligocene|Silicified infill of the Stuart Creek Palaeovalley. Rich in fossilised plant material. Probably equivalent to the Oligo-Miocene sands of the Poole Creek palaeovalley.||||||08-APR-16
25626|Willalinchina Sandstone|66131|6|Mentioned|p242 Fig.2|Pliocene|Eocene|Middle Eocene to early Pliocene in age (from p.242 Fig.2 - stratigraphic correlation chart).||||||
25626|Willalinchina Sandstone|66623|6|Mentioned|p273.|||Billa Kalina Basin, South Australia. Part equivalent to Eyre Formation.||||||
25626|Willalinchina Sandstone|67462|5|Briefly described|Map legend.|Pliocene|Pliocene|Billa Kalina Basin.||||||
25626|Willalinchina Sandstone|68715|6|Mentioned|p30 Fig.5|Zanclean|Messinian|Billa Kalina Basin.||||||
39177|Willamulka Volcanics Member|24475|2|Defined|p55|Paleoproterozoic|Paleoproterozoic|Of Matta Formation. Formerly Willamulka Volcanics.||||||07-NOV-08
39177|Willamulka Volcanics Member|65375|6|Mentioned|p19, p21, p23.|||||Unit in Matta Formation.|||Amygdaloidal mafics.|
39177|Willamulka Volcanics Member|65376|6|Mentioned|p101 Fig.3.1.|||||||||
39177|Willamulka Volcanics Member|66302|6|Mentioned|p33|||Olympic Domain, Gawler Craton. ||||||
24574|Willawalpa Formation|22772|5|Briefly described|Table13.1|Cryogenian|Cryogenian|||||||
24574|Willawalpa Formation|22857|5|Briefly described|Tb. 13.1 (insert p70-71)|Torrensian|Torrensian|Of the River Wakefield Subgroup (Burra Group).||||||
24574|Willawalpa Formation|22869|6|Mentioned|P46|||Correlated to the Carey Gully Sandstone Member||||||
24574|Willawalpa Formation|22889|6|Mentioned|p31|Adelaidean|Adelaidean|Parent - Emeroo Subgroup.  Former Parent Unit - River Wakefield Subgroup, see p33 for details on change.||||||
24574|Willawalpa Formation|24175|4|Described|p11|Neoproterozoic|Neoproterozoic|of Emeroo Subgroup (Burra Group).  Overlain transitionally by Witchelina Quartzite; underlain conformably by Top Mount Sandstone Beds.   Max. thickness: 2242m.||||||
24574|Willawalpa Formation|24321|5|Briefly described|Map legend|Adelaidean|Adelaidean|Parent: Emeroo Subgroup||||||
24574|Willawalpa Formation|37854|2|Defined|p14|Adelaidean|Adelaidean|See also P13.Prob.Early Torrensian||||||
24574|Willawalpa Formation|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Torrensian||||||
24574|Willawalpa Formation|41403|6|Mentioned|p43|||||||||
24574|Willawalpa Formation|41404|4|Described|p93|||||||||
24574|Willawalpa Formation|42222|6|Mentioned|p13|||||||||
24574|Willawalpa Formation|42238|5|Briefly described|p78|||||||||
24574|Willawalpa Formation|43052|5|Briefly described|p177,Table 6.1|||of River Wakefield Subgroup||||||
24574|Willawalpa Formation|60718|5|Briefly described|p49 Fig. 2|Adelaidean|Adelaidean|Geological Province: Adelaide Geosyncline. See also p51 Fig. 3.||Of Emeroo Subgroup (Burra Group).||||15-APR-11
24574|Willawalpa Formation|66884|5|Briefly described|p39 Fig.2, p41 Fig.3|||Thickness: up to 2250 m.||Emeroo Subgroup||Overlies Top Mount Sandstone beds; is overlain by Witchelina Quartzite.|Quartz arenite (thin-bedded, flaggy, ripple cross-laminations, shale intraclasts, desiccation cracks, cross-bedding and lenticular bedding); interbedded with subordinate siltstone (dark grey); rare stromatolitic dolostone (dark grey).|14-DEC-16
24574|Willawalpa Formation|69019|3|Fully described|p38-39.|Neoproterozoic|Neoproterozoic|Proposed by Murrell (1977); defined by Forbes et al. (1981). Type section NE of Kingston Dam where it is 2,242 m thick. Displays a variety of shallow-water and evaporitic sedimentary structures.||Unit in Emeroo Subgroup.||Overlies Top Mount Sandstone Beds conformably. Is overlain transitionally by Witchelina Quartzite.|Thin interbeds of grey siltstone, brown stromatolitic dolomite and pale brown flaggy to platy bedded sandstone with a coarse-grained texture; mud rip-up clasts common.|
24574|Willawalpa Formation|72456|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Marree 1:250k map sheet. |||||Sandstone, pale brown, coarse-grained, siltstone, sandy, dolomite, stromatolitic.|
26216|Willawortina Formation|23155|6|Mentioned|p36|||The unit is not recognised on STRZELECKI but can probably be equated with the Yandruwantha Sand.||||||
26216|Willawortina Formation|24102|5|Briefly described|p132|Pliocene|Late Miocene|Maximum Thickness: >140 m.||||||30-NOV-04
26216|Willawortina Formation|24566|5|Briefly described|p113|Pliocene|Miocene|Coarse clastics. Max. thickness: >140m.||||||
26216|Willawortina Formation|30055|6|Mentioned|p154|||Minerology P159.||||||
26216|Willawortina Formation|30056|2|Defined|p133|early Pleistocene|late Miocene|Late Miocene to Early Pleistocene||||||
26216|Willawortina Formation|30920|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
26216|Willawortina Formation|32121|6|Mentioned|p422|||||||||
26216|Willawortina Formation|34882|6|Mentioned|p88|||||||||
26216|Willawortina Formation|36620|5|Briefly described|Fig.1|||See also p24.||||||17-SEP-18
26216|Willawortina Formation|38605|6|Mentioned|p31|||||||||
26216|Willawortina Formation|39902|6|Mentioned|Fig.5|||||||||
26216|Willawortina Formation|40373|6|Mentioned|p36|||||||||
26216|Willawortina Formation|40381|6|Mentioned|Fig.7|||||||||
26216|Willawortina Formation|40756|5|Briefly described|p3|||||||||
26216|Willawortina Formation|40757|6|Mentioned|p76|||||||||
26216|Willawortina Formation|41125|6|Mentioned|Table 10|||||||||
26216|Willawortina Formation|41537|6|Mentioned|Fig.2|||||||||
26216|Willawortina Formation|42090|3|Fully described|p37|||||||||
26216|Willawortina Formation|42205|5|Briefly described|p254|||See also Fig.1||||||
26216|Willawortina Formation|42391|5|Briefly described|p78|||||||||
26216|Willawortina Formation|42543|6|Mentioned|p6|||||||||
26216|Willawortina Formation|42746|5|Briefly described|Fig.9 P14|||||||||
26216|Willawortina Formation|42813|6|Mentioned|p25|||||||||
26216|Willawortina Formation|42957|6|Mentioned|p40|||||||||
26216|Willawortina Formation|43053|5|Briefly described|Map Legend|Pleistocene|Pleistocene|||||||25-MAY-05
26216|Willawortina Formation|43258|5|Briefly described|Map Legend|Holocene|Pleistocene|||||||
26216|Willawortina Formation|43298|6|Mentioned|Map Legend|Holocene|Pleistocene|||||||
26216|Willawortina Formation|44133|5|Briefly described|p242, 244 Table 11.3|Pleistocene|Pliocene|Correlated with the Avondale Clay. Maximum Thickness: 100m. ||||||
26216|Willawortina Formation|46815|6|Mentioned|p249|||||||||
26216|Willawortina Formation|46833|6|Mentioned|p53|||||||||
26216|Willawortina Formation|60564|5|Briefly described|p4, p6|||Overlies the Namba Formation and the Beverley Clay. Composed of clay, sand and gravel.||||||
26216|Willawortina Formation|60953|5|Briefly described|Map Legend|Pleistocene|Pliocene|Alluvial sandy clay and gravel, often calcreted.||||||
26216|Willawortina Formation|60959|5|Briefly described|Map Legend|Pleistocene|Pliocene|Calcareous sandy to silty clay, and medium grained snad grading to boulder deposits.||||||
26216|Willawortina Formation|61108|5|Briefly described|map legend|Pleistocene|Pliocene|Alluvial sandy clay and gravel, often calcreted.||||||01-JUN-05
26216|Willawortina Formation|61155|5|Briefly described|p17|||Age: ~13-2.5Ma. Thickness: 150m.  Geological Province: Tarkarooloo Basin.||||||
26216|Willawortina Formation|65194|5|Briefly described|p37, p47-48|Early Pleistocene|Miocene|Comprises up to 150m of alluvial fan deposits. Overlies the Namba Formation; overlain by Quaternary age colluvial, fluvial and aeolian sediments.||||||
26216|Willawortina Formation|65925|5|Briefly described|pp17-18, p21, p136, Appendix 2.|||Formed as piedmont fans around Flinders and Olary Ranges. Has a fine and a coarse facies. Up to 100m thick.||||Overlies Namba Formation. Is overlain locally by Eurinilla Formation in incised paleochannels.|Fine facies: upwards fining cyclical sequence of sandy mud and silty dolomite with distal clay and calcareous paleosols. Coarse facies: coarse gravels and debris flows.|
26216|Willawortina Formation|66131|6|Mentioned|p240, p244 Fig.4, p245-246|Quaternary|Pliocene|Of Callen and Tedford (1976); Callen (1977). Flanking northern Flinders Ranges. Channel and debris flow processes.|||||Fine sandy mud and silty dolomite; coarse piedmont clastics: clast supported gravel and poorly sorted clayey gravel.|
26216|Willawortina Formation|66303|6|Mentioned|pp27-28, p31 Fig.5.|Paleogene|Paleogene|Lake Eyre Basin.||||||
26216|Willawortina Formation|66518|5|Briefly described|p19 Fig.4, p20.|Cenozoic|Cenozoic|Lake Eyre Basin. Late Neogene uplift of the Flinders Ranges produced these fluvial/colluvial sediments.||||Overlies, possibly unconformably, Namba Formation. Is overlain by Eurinilla Formation and equivalents. Is shown as age-equivalent to lower part of Millyera Formation.||
26216|Willawortina Formation|68068|5|Briefly described|Map legend|Pliocene|Late Miocene|Callabonna Sub-basin, Lake Eyre Basin. Piedmont slope deposit. Stratigraphic unit age Miocene - Pliocene, with pedogenic carbonate in upper layers >43,000 years BP(radiogenic).||||Is overlain by, locally intertongues with, Millyera Formation.|Calcareous, silty to sandy clay and medium sand grading to boulder deposits near ranges; interbedded greenish pebbly or sandy carbonates; poorly sorted, cross-bedded; greenish-brown carbonate nodules common.|25-NOV-14
26216|Willawortina Formation|68203|6|Mentioned|p9 Fig.6|||Mount Lofty Ranges.||||Is faulted against Eyre Formation.||
26216|Willawortina Formation|68715|6|Mentioned|p32 Fig.6|Quaternary|Quaternary|||||||
26216|Willawortina Formation|69023|4|Described|p101, p109, p124-126, p133|Pleistocene|Pleistocene|Of Callen and Tedford (1976). Overlies lower Namba Formation, and intertongues with the upper Namba Formation. Records alluvial fan deposits from the beginning of Cenozoic uplift of the Flinders Ranges. c.13m thick. Age discussed.||||Overlies Namba Formation and Yandruwantha Sand. Is overlain by Eurinilla Formation, and by Millyera Formation locally. Intertongues with Millyera Formation. Correlated with Avondale Clay.|Extremely to very poorly sorted bouldery to pebbly silt and greenish clay with numerous greenish carbonate nodules; lenses and sheets of dolomite; stringers and lenses of sand to boulders. Gypsum crust in upper 1-2m.|
26216|Willawortina Formation|69562|6|Mentioned|p662 Tb.2, p666-668, p675|Pliocene|Pliocene|Electrical conductivity value used in forward modelling: 50 mS/m.|c.6 - 4 Ma.|||Unconformably overlies Namba Formation.||06-APR-22
26216|Willawortina Formation|69568|5|Briefly described|p443-444|Quaternary|Quaternary|Lake Frome region, Lake Eyre Basin. Deposited during late Cenozoic to Plio-Pleistocene uplift and exposure of the Mount Painter Domain.||||Overlies Namba Formation.|Coarse siliciclastics, from braided fans and fine sands to clays from lacustrine settings.|
26216|Willawortina Formation|70339|5|Briefly described|map legend|Pleistocene|Pliocene||||||Sandy mud; silty dolomite, lacustrine, flooplain. Coarse framework supported gravel, braided flow origin and matrix supported clayey gravels (debris flows).|
26216|Willawortina Formation|70340|5|Briefly described|map legend|Pleistocene|Pliocene||||||Sandy mud, silty dolomite, lacustrine, floodplain. Coarse framework supported gravel, braided flow origin and matrix supported clayey gravels (debris flow).|
26216|Willawortina Formation|70383|5|Briefly described|p45|Holocene|Neogene|Lake Eyre Basin margins. Colluvial and fluvial sediments.||||||
26216|Willawortina Formation|70384|5|Briefly described|Map legend.|Pliocene|Miocene|Piedmont slope deposit. Stratigraphic age is Late Miocene-Pliocene; pedogenic carbonate in upper layers is >43,000 years BP.|||||Calcareous, silty to sandy clay and medium sand grading to boulder deposits near ranges; interbedded greenish pebbly or sandy carbonates; poorly sorted, cross-bedded in coarser fraction, crude horizontal stratification. Carbonate nodules common.|
26216|Willawortina Formation|72457|5|Briefly described|p91|Pleistocene|Pleistocene|Callabonna sub-basin.|||||Lacustrine and piedmont deposits.|
26216|Willawortina Formation|72458|6|Mentioned|p4-5|Quaternary|Pliocene|Alluvial fan sequence.||||Underlain by Namba Formation.|Gravels and fanglomerates.|
26216|Willawortina Formation|73251|5|Briefly described|p36-37, p39, p41-42, p45, p57, p59-62|Pleistocene|Pliocene|Lake Eyre Basin, Callabonna Sub-basin / Poontana Trough. Thermally sub-mature. Interpreted as alluvial fans and interfluves that developed on the margins of the Flinders Ranges and incorporated scree from uraniferous crystalline basement. Decreases in thickness and grain size away from the Mount Painter Inlier. Greatest thickness [reported here]: 102 m.||||Unconformably[?] underlain by Namba Formation. Overlain by Eurinilla Formation. Equivalent to Millyera Formation.||
25630|Wilmington Formation|22510|5|Briefly described|p39|||Of the Upalinna Subgroup.  Age: Marinoan.||||||13-OCT-04
25630|Wilmington Formation|23250|5|Briefly described|p1124 Fig.2||Cryogenian|Actually referred to as Wilmington Formation equivalent. This equivalent correlating to Yaltipena Formation, Trezona Formation, Enorama Shale (Umberatana Group) and Olympic Formation.||||||
25630|Wilmington Formation|23818|5|Briefly described|p64 Fig.22, p70|Adelaidean|Adelaidean|Of the Willochra Sub-Group. Max. thickness: ~1500 ft.||||||
25630|Wilmington Formation|24176|6|Mentioned|p12|Adelaidean|Adelaidean|Of the Willochra Sub-Group.  Age is Marinoan.||||||
25630|Wilmington Formation|30177|6|Mentioned|p83|||||||||
25630|Wilmington Formation|30801|6|Mentioned|p5|||Marinoan. Table P5-6||||||
25630|Wilmington Formation|30802|6|Mentioned|p14|||||||||
25630|Wilmington Formation|30807|6|Mentioned|p103|||Suggested map stmbol||||||
25630|Wilmington Formation|32506|6|Mentioned|Fig.1|||||||||
25630|Wilmington Formation|32510|6|Mentioned|Fig.1|||||||||
25630|Wilmington Formation|33422|6|Mentioned|Map legend|Precambrian|Precambrian|||||||
25630|Wilmington Formation|33423|4|Described|p13|||||||||
25630|Wilmington Formation|33474|6|Mentioned|Fig.2|||||||||
25630|Wilmington Formation|34521|5|Briefly described|p156|||||||||
25630|Wilmington Formation|34535|4|Described|p70|||Marinoan. See Fig.22||||||
25630|Wilmington Formation|34536|6|Mentioned|Map legend|Adelaidean|Adelaidean|Marinoan||||||
25630|Wilmington Formation|35255|6|Mentioned|Fig.7|||||||||
25630|Wilmington Formation|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Marinoan||||||
25630|Wilmington Formation|39351|6|Mentioned|Map legend|Adelaidean|Adelaidean|Marinoan||||||
25630|Wilmington Formation|40456|6|Mentioned|Fig.2|||||||||
25630|Wilmington Formation|41403|6|Mentioned|p56|||||||||
25630|Wilmington Formation|41405|3|Fully described|p180|||||||||
25630|Wilmington Formation|41526|6|Mentioned|p62|||||||||
25630|Wilmington Formation|42222|6|Mentioned|p17|||||||||
25630|Wilmington Formation|42239|6|Mentioned|p149|||||||||
25630|Wilmington Formation|42542|6|Mentioned|Fig.4 P14|||||||||
25630|Wilmington Formation|42882|5|Briefly described|Fig.7 P12|||Of Umberatana Group.||||||30-SEP-08
25630|Wilmington Formation|43052|5|Briefly described|p189,Table 6.1|||Of Willochra Subgroup.||||||30-SEP-08
25630|Wilmington Formation|60959|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Of the Upalinna Subgroup. Red-brown micaceous siltstone with fine sandstone interdbeds.||||||
25630|Wilmington Formation|61732|5|Briefly described|p28 Fig. 13|Marinoan|Marinoan|Of the Upalinna Subgroup (Umberatana Group). Includes the Marino Arkose Member. Geological Province: Adelaide Rift Complex.||||||07-FEB-11
25630|Wilmington Formation|64797|5|Briefly described|p161, p166 Tb.7, p168 Tb.11|||S-isotope data.||||||
25630|Wilmington Formation|67030|5|Briefly described|p408, p409 Fig. 2|Cryogenian|Cryogenian|Shown as lateral equivalent to Enorama Shale and Waukaringa Siltstone.|657 +/- 17 Ma (zircon, Ireland et al. 1998)|Willochra Subgroup||Overlies Angepena Formation, underlies Elatina Formation.||26-APR-12
25630|Wilmington Formation|70031|5|Briefly described|p246|Cryogenian|Cryogenian|Adelaide Geosyncline. Partial equivalent to Enorama Shale.|||Includes Marino Arkose Member.|||
25630|Wilmington Formation|70082|5|Briefly described|p2-3,15|Cryogenian|Cryogenian|Kulpara-Adelaide region, with equivalents in the Stuart Shelf. Contains a detrital zircon dated by U-Pb at 657+\-17 Ma (Ireland et al., 1998).|||Includes Marino Arkose Member.|Underlain unconformably by Tapley Hill Formation.||
25630|Wilmington Formation|70333|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic||||||Sandstone, red, grey, with grit bands and gritty limestone; siltstone, red, gritty.|
25630|Wilmington Formation|70334|4|Described|p2,20,27-28, 30, 38,47,51-53,77,81|Neoproterozoic|Neoproterozoic|Geological province: Gawler Craton. Of Adelaide Geosyncline and Stuart Shelf. Thickness: 20-55m on CULTANA. Transgressive-regressive sequence. Reflects influx of coarse detritus into the basin frin Gawler Craton after shallow-water deposition of the underlying Angepena Formation. Basal conglomerates contains clasts derived of dolomite, BIFS and sandstone from Pandurra Formation, felsic volcanics from Gawler Range Volcanics. Deposited in a shallow marine to tidal environment.||Unit of Upalinna Subgroup.||Conformably underlain by Angepena Formation. Overlain by the Whyalla Sandstone.|Fine- to medium-grained grey-green sandstones interlayered with coarse-grained lithic sandstone, grey-green to red-brown siltstone and dolomite, basal conglomeratic beds.|14-OCT-19
25630|Wilmington Formation|71129|5|Briefly described|p15,107,110,114,116-118,208|Cryogenian|Cryogenian|Of Adelaide Geosyncline. Clastic sedimentation in a shallowing rift during Marinoan Epoch; shallow water, possibly tidally influenced marine environments. Thickness may reach up to 20m thick in drillholes (cf. McAvaney et al., 2014).||||Underlain by Angepena Formation. Correlable with Yudnapinna Beds.||
25630|Wilmington Formation|72247|6|Mentioned|p41|Neoproterozoic|Neoproterozoic|Of Adelaide Geosyncline.||||||
25630|Wilmington Formation|72450|5|Briefly described|Brochure, Brochure map|||Forms sea cliffs south from Marino and is the bedrock under the northern parts of the McLaren Vale Wine Region.Deformed by the Delamerian Orogeny.||Umberatana Group||Overlain by the Reynella Siltstone Member.|Grey-green laminated siltstone passing up into massive fine-grained sandstone.|
25630|Wilmington Formation|73110|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic||||||Sandstone, red, grey, with grit bands and gritty limestone; siltstone, red, gritty.|
25630|Wilmington Formation|73188|5|Briefly described|p316, p330-331, p357|Neoproterozoic|Neoproterozoic|Mount Lofty Ranges.||Upalinna Subgroup, Umberatana Group|||Green siltstone and massive sandstone.|
25630|Wilmington Formation|73227|6|Mentioned|p36|||Adelaide Superbasin. May have been a lateral fluid conduit.||||||
25630|Wilmington Formation|73234|6|Mentioned|p6|||Deposited in shallow marine to tidal flat environments.|||||Silty to sandy.|
25630|Wilmington Formation|73236|4|Described|p35-41, p43, p45, p47|Cryogenian|Cryogenian|Marine shelf sedimentary rocks. Oldest in situ rocks in the Hallett Cove area; exposed, albeit intermittently, along Waterfall Creek. Slaty cleavage is developed in the fine-grained siltstones at Hallett Cove. Transgressive-regressive sequence.|c. 645-640 Ma|Upalinna Subgroup, Umberatana Group, Heysen Supergroup|Marino Arkose Member|Underlain by Angepena Formation. Overlain by Elatina Formation (Yerelina Subgroup).|Green-grey siltstone and fine-grained sandstone, partly with ripple marks and small-scale cross-bedding.|
25630|Wilmington Formation|74367|5|Briefly described|p7 Fig.6, p8-9, p11, p14, p16-17, p22|Cryogenian|Cryogenian||688+/-8 Ma LA-ICP-MS detrital zircon MDA||Marino Arkose Member|||
35857|Wilunga Formation|23331|5|Briefly described|1089 Fig.2|Early Oligocene|Early Oligocene|||||||
24109|Wimma Sandstone Member|13497|4|Described|v, vi, viii, xii, p69 fig 6.1|Anisian|Scythian|Cooper Basin. Originally defined by Powis (1989) before being redefined by Channon and Wood (1989). Reference sections nominated by Powis (1989) and Channon and Wood (1989). More than 100m thick in the Patchawarra trough and reaches a maximum thickness of 114m in Potiron 1. Petrography is briefly discussed. Reservoir and outcrop characteristics are discussed. Deposited by low-sinuosity river systems. See also p104-p105, p110-p112, p157 tbl 10.1, p159, p161, p166, p167 fig 10.10.||Arrabury Formation||Equivalent to the Paning Member. Overlies the Callamurra Member and the Paning Member. Conformably overlain by the Tinchoo Formation.|Buff to pale grey, fine to medium-grained quartzose sandstone with minor interbeds of pale to medium grey siltstone and mudstone.|
24109|Wimma Sandstone Member|13516|5|Briefly described|p171 fig 12|Early Triassic|Early Triassic|In Eromanga Basin.||Of Arrabury Formation||||
24109|Wimma Sandstone Member|22839|6|Mentioned|P33|||||||||
24109|Wimma Sandstone Member|22883|6|Mentioned|P29|||Parent is Arrabury Formation.||||||17-SEP-08
24109|Wimma Sandstone Member|23155|6|Mentioned|Fig 8 on p16|||||||||
24109|Wimma Sandstone Member|23375|4|Described|Fig2 p265,280||Spathian|Of the Arrabury Formation. Geological province: Cooper Basin.||||||17-JAN-08
24109|Wimma Sandstone Member|24210|5|Briefly described|p133 Fig. 2|Middle Triassic|Early Triassic|Of the Arrabury Formation (Nappamerri Group).  Geological Province: Cooper Basin.||||||
24109|Wimma Sandstone Member|42008|3|Fully described|PP271|Anisian|Scythian|Of the Arrabury Formation.||||||17-JAN-08
24109|Wimma Sandstone Member|42085|6|Mentioned|Fig.2 P374|||||||||
24109|Wimma Sandstone Member|43628|6|Mentioned|Fig.13|||||||||
24109|Wimma Sandstone Member|44133|5|Briefly described|p65 Fig. 8.3, 86|Triassic|Triassic|Of the Arrabury Formation. Geological Province: Cooper Basin. Overlies: Paning Member ). Overlain by the Tinchoo Formation.||||||
24109|Wimma Sandstone Member|60717|5|Briefly described|p40 Fig. 2|Anisian|Scythian|Of Arrabury Formation (Nappamerri Group). Overlies and interfingers with Paning Member of the same unit. Thickness: 100m. Geological Province: Cooper Basin.||||||31-JAN-08
24109|Wimma Sandstone Member|61613|5|Briefly described|p282 Fig. 2|Early Triassic|Early Triassic|Sandstone is Sst in Fig. 2. Of Arrabury Formation. Overlain by Doonmulla Member, Underlain by Paning Member. Geological Province: Cooper and Simpson Basins.||||||18-JUL-14
24109|Wimma Sandstone Member|61615|6|Mentioned|p302 Fig. 2|Middle Triassic|Early Triassic|Of Nappamerri Group. Geological Province: Cooper Basin.||||||07-FEB-11
24109|Wimma Sandstone Member|61616|6|Mentioned|p330 Fig. 2|Early Triassic|Early Triassic|Of Arrabury Formation. Geological Province: Cooper Basin.||||||
24109|Wimma Sandstone Member|62730|5|Briefly described|p352 Fig. 1|Middle triassic|Early Triassic|Of the Arrabury Formation. Geological Province: Cooper Basin.||||||21-APR-08
24109|Wimma Sandstone Member|63978|2|Defined|p22, Fig. 3|Middle Triassic|Early Triassic|Of Powis (1989). Of Arrabury Fm. Conformable on Paning Mbr; unconformable below Tinchoo Fm. Mainly finely interbedded sandstone with pale to medium grey siltstone; mudstone is buff to pale grey, fine- to medium-grained, quartzose. In the Cooper Basin.||||||07-FEB-11
24109|Wimma Sandstone Member|64048|5|Briefly described|p67|||Within the upper Arrabury Formation. Consists dominantly of fine- to medium-grained quartzose sandstone with minor interbeds of medium-grey siltstone and mudstone. Contains oil.||||||07-FEB-11
24109|Wimma Sandstone Member|64197|6|Mentioned|p625 Fig.1c|Middle Triassic|Early Triassic|Appears only as Wimma in Fig.1c. Cooper Basin||Unit in Arrabury Group.||Overlies Paning Member. Is overlain by Tinchoo Formation.||
24109|Wimma Sandstone Member|64665|5|Briefly described|p53 Fig.2.|Middle Triassic|Middle Triassic|Cooper Basin.||Top unit in Arrabury Formation.||Overlies Paning Member.||
24109|Wimma Sandstone Member|65489|5|Briefly described|p48, p96, p131-132|Anisian|Scythian|100m thick. Hosts economic oil and gas reservoirs.||Topmost unit in Arrabury Formation.||Overlies Paning and Callamurra Members. Is overlain by Tinchoo Formation.||
24109|Wimma Sandstone Member|67402|5|Briefly described|p90, p90 fig CPR4|||Probably a facies equivalent of the Paning Member. Deposited in a fluvial environment. Generally regarded as a poor-quality reservoir but may form a structural trap. Generally greater than 100m thick. See also p91 tbl CPR1, p94, p99 fig CPR14, p100, p101, p101 tbl CPR2, p105.||Arrabury Formation||Conformably overlies the Paning Member. Unconformably overlain by the Doonmulla Member.|Stacked medium to fine-grained sandstones with finely interbedded siltstones and mudstones.|
24109|Wimma Sandstone Member|68731|5|Briefly described|p200 Fig 3.110, p207, pp209-211|Middle Triassic|Lower Triassic|Cooper Basin. Powis (1989). Up to 100 m thick. Deposition occurred in weakly sinuous rivers. Limited palynological data indicate late Olenekian-early Anisian (Gray and McKellar 2002).||Of the Arrabury Formation.||Unconformably overlain by the Tinchoo Formation. Conformably underlain by the Paning Member.|Comprises fine to medium, quartzose sandstone with minor interbeds of siltstone and mudstone.|
24109|Wimma Sandstone Member|69797|5|Briefly described|p17 Fig.2|Middle Triassic|Early Triassic|Age: Scythian - Anisian (approximated from figure). Geol. Prov: Cooper Basin.||Arrabury Formation||||
24109|Wimma Sandstone Member|69946|5|Briefly described|p9, p36, p54|Anisian|Scythian|Cooper Basin.||Unit in Arrabury Formation.||Overlies Paning Member. Is overlain by Doonmulla Member (Tinchoo Formation).||
24109|Wimma Sandstone Member|69947|5|Briefly described|p13 Fig.7.2|Middle Triassic|Early Triassic|Cooper Basin.||Arrabury Formation.||||
24109|Wimma Sandstone Member|70317|6|Mentioned|p33|Middle Triassic|Early Triassic|Cooper Basin.||Arrabury Formation.||Overlies Paning and Callamurra Members. Is overlain by Tinchoo Formation.||
24109|Wimma Sandstone Member|70823|5|Briefly described|p40, p75-p76, p79, p81|||Cooper Basin. Contains economic oil and gas reservoirs locally.||Arrabury Formation||Overlies the Callamurra and Paning Members.|Sandstone with minor siltstone interbeds.|
24109|Wimma Sandstone Member|70824|4|Described|p7, p104|Olenekian|Olenekian|Cooper Basin. Deposited in braided fluvial channels and floodplain environments.||Arrabury Formation||Conformably overlies the Paning Member. Overlain by the Tinchoo Formation.|Sandstone with minor siltstone interbeds.|
24109|Wimma Sandstone Member|70946|5|Briefly described|p1089|Middle Triassic|Early Triassic|Cooper Basin. Deposited in a braided fluvial channel belt and floodplain environment.||Arrabury Formation.||||08-OCT-18
24109|Wimma Sandstone Member|71342|6|Mentioned|Ch5 p9, Ch5 p36, Ch5 p54, Ch7 p13|Anisian|Scythian|Cooper Basin. Palynological zone is given in fig 5.3 Ch5 p36. Deposited in a braided fluvial channel or floodplain environment.||Arrabury Formation||Overlies the Paning Member. Overlain by the Tinchoo Formation.||
24109|Wimma Sandstone Member|73167|6|Mentioned|p664 Fig. 2|Triassic|Triassic|Cooper Basin. Contains oil and gas.||Nappamerri Group||||
24109|Wimma Sandstone Member|73244|6|Mentioned|p86|Triassic|Triassic|Cooper Basin.  Along with Callamurra Member, Panning Member and Tinchoo Formation, shown as floodplain, lacustrine, fluvial channels. Oil and gas.||||||
24109|Wimma Sandstone Member|73251|6|Mentioned|p62|Middle Triassic|Early Triassic|Cooper Basin. Braided fluvial channel belt and floodplain depositional environments. Contains[?] gas and oil.||Arrabury Formation, Nappamerri Group||Underlain by Callamurra Member. Underlain by and equivalent to Paning Member. Overlain by Tinchoo Formation.||
24109|Wimma Sandstone Member|73343|6|Mentioned|p337|Triassic|Triassic|Cooper Basin. Hosts oil and gas.||Nappamerri Group||Underlain by Panning Member. Overlain by Tinchoo Formation.||
24109|Wimma Sandstone Member|73479|5|Briefly described|p156 Fig.2, p159|Triassic|Triassic|Cooper Basin. Floodplain, lacustrine, fluvial channels depositional environment.|ca 241 Ma|Nappamerri Group||Overlies Panning Member, underlies Tinchoo Formation||
75888|Windamerta Diorite|67540|2|Defined|pp25-28 Fig.1,Tb.1; p36, p37, p38 Fig.2|Calymmian|Calymmian|New name. Type locality: 1 km SE of Mount Victoria extending ~1.3 km to SE. Curnamona Province, Western Olary Domain. Definition reference: this article and Fricke and Hore (2011). A more recent age is 1581 +/- 6 Ma (SHRIMP I: Fanning, ANU). Windamerta Diorite post-dates mineralisation.|1577 +/- 66 Ma (U-Pb: Ludwig and Cooper 1984).|Of the Ninnerie Supersuite.||Intermingled with the Crocker Well Suite.|Biotite and hornblende diorites to granodiorites with plagioclase, K-feldspar, quartz and retrograde chlorite.|05-FEB-16
75888|Windamerta Diorite|69562|5|Briefly described|p672 Tb.5|||Magmatic crystallisation age.|1581 +/- 6 Ma (Fanning).||||Biotite and hornblende diorites, granodiorites and tonalites.|06-APR-22
75888|Windamerta Diorite|69650|2|Defined|p4 Tb.1, p2, p6, p11-12, p22-23, p28-32|Calymmian|Calymmian|New name, after Windamerta Hill, 56 km NW of Manna Hill. Western Olary Domain, Curnamona Province. Good outcrop exposure approximately 1.5 km SE Mount Victoria Hut, GDA 94, 389600 mE, 6461600 mN (Fig. 8) extending 1.3 km in a SE direction.  Geochronology, geochemistry outlined. Misspelt p21.|1581 +/- 6 Ma and 1577 +/- 66 Ma.|Unit in Ninnerie Supersuite.||Intimate mingling with Crocker Well Suite.|Biotite and hornblende diorites to granodiorites with plagioclase, K-feldspar, quartz and retrograde chlorite. I-type.|08-DEC-22
75888|Windamerta Diorite|70339|5|Briefly described|map legend|Mesoproterozoic|Mesoproterozoic||1581+/-6 and 1577+/-66 [typo in error range?] Ma.|Ninnerie Supersuite.|||Diorite to granodiorite, prominent biotite and hornblende, with plagioclase, K-feldspar, quartz and retrograde chlorite; I-type.|02-FEB-16
75888|Windamerta Diorite|70658|5|Briefly described|p33-36|Mesoproterozoic|Mesoproterozoic|Restricted to Plumbago Inlier, western Olary Domain, Curnamona Province. Geochemistry briefly described. Locally (Outalpa Inliers) co-mingled with other granites of the Bimbowrie Suite.|1581 +/- 6 Ma and 1577 +/- 66 Ma.||||Biotite and hornblende diorites to granodiorites with plagioclase, K-feldspar, quartz and retrograde chlorite. I-type.|
24633|Winnitinny Creek Member|40431|2|Defined|p16|Early Cambrian|Early Cambrian|Misspelling of Winitinny Creek Member?[?Winnitinny is the correct spelling!] Atdabanian.||||||
24633|Winnitinny Creek Member|40831|6|Mentioned|p2|||||||||
24633|Winnitinny Creek Member|42233|6|Mentioned|p252|||See also Fig.2||||||
24633|Winnitinny Creek Member|67907|6|Mentioned|p257, p259-260|||Flinders Ranges. Contains the A. huoi trilobite zone[?].||||||
24633|Winnitinny Creek Member|69570|5|Briefly described|p423-p426, p428, p430, p432-p434|||Arrowie Syncline, Flinder Ranges. Over 135m thick and represents a change from moderate to high energy shallow water platform to restricted, low-energy, intrashelf and possibly deeper lagoonal environment. Fossil assemblage and sample localities are described.||||Overlies the Hideaway Well Member. Interfingered with and partially overlain by, the Wirrapowie Limestone. Partially equivalent to the Ajax Limestone.|Massive carbonate, bioclastic grainstones alternating with micritic and microbial laminated carbonates.|
24633|Winnitinny Creek Member|70833|5|Briefly described|p180-181,183,185-188,190-199,201|Series 2|Terreneuvian|Of Arrowie Basin. Key sections: MORO (S of Moro Gorge, Arrowie Syncline); BALC (Balcoracana Gorge, Bunkers Range); MMT (Bunkers Range, central Flinders Ranges); WILK (Bunkers Graben); 10MS-W (Ten Mile South, SE Bunkers Graben). Truncated in places on the shallow carbonate shelf by a red karstified surface, representing the regionally significant hiatus "Flinders Unconformity". Includes M. etheridgei zone in upper part of the section. Correlable to Fork Tree Limestone in the Stansbury Basin.||Unit of Wilkawillina Limestone.||Conformably underlain by Hideaway Well Member.||08-AUG-19
24633|Winnitinny Creek Member|70835|6|Mentioned|p336-337, 351|Cambrian|Cambrian|Arrowie Basin, Flinders Ranges.||Wilkawillina Limestone.||Overlies Hideaway Well Member. Is overlain unconformably by Third Plain Creek Member or Six Mile Bore Member (Mernmerna Formation).||
24633|Winnitinny Creek Member|71102|5|Briefly described|p245, p251,267,275|Series 2|Terreneuvian|Of Arrowie Basin.||Unit of Wilkawillina Limestone.||Uppermost unit of Wilkawillina Limestone. Underlain by Hideaway Well Member.||05-SEP-19
70231|Winnowie Member|64460|5|Briefly described|p198|||Of Rawnsley Quartzite. Thickness: 90m. Suite of channel deposits. See p198 fo more information.||||||27-JAN-09
27008|Wintrena Formation|22613|4|Described|p26|||||||||
27008|Wintrena Formation|22614|5|Briefly described|map|Pleistocene|Pleistocene|||||||
27008|Wintrena Formation|38604|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
27008|Wintrena Formation|38605|4|Described|p31|||See also Table 5.||||||
27008|Wintrena Formation|40912|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
27008|Wintrena Formation|42816|4|Described|p27|||||||||
27008|Wintrena Formation|43053|5|Briefly described|Map Legend|Quaternary|Quaternary|||||||25-MAY-05
27008|Wintrena Formation|43258|5|Briefly described|Map Legend|Holocene|Pleistocene|||||||
27008|Wintrena Formation|43298|6|Mentioned|Map Legend|Holocene|Pleistocene|||||||
27008|Wintrena Formation|44133|5|Briefly described|p251|Quaternary|Quaternary|Thickness: 20m. ||||||
27008|Wintrena Formation|44695|5|Briefly described|Map Legend||Pleistocene|||||||
27008|Wintrena Formation|60953|5|Briefly described|Map Legend|Holocene|Pleistocene|Aeolian sand of inland dune fields. Includes associated alluvial and regolith materials in interdunal areas.||||||28-APR-05
27008|Wintrena Formation|61108|5|Briefly described|map legend|Quaternary|Quaternary|Aeolian sand of inland dune fields. Includes associated alluvial and regolith materials (including calcrete) in interdunal areas.||||||
27008|Wintrena Formation|61155|5|Briefly described|p17|Pleistocene|Pleistocene|Overlain by Benitos Clay. Thickness: 8m. Geological region: Oodnadatta area.  ||||||
27008|Wintrena Formation|62961|5|Briefly described|p15|Late Pleistocene|Late Pleistocene|Dune-forming unit in the Great Victoria Desert.  Commonly contains a number of secondary calcrete horizons that may be geochemically anomalous in several metals.||||||
27008|Wintrena Formation|69648|5|Briefly described|p29-30, map legend|Pleistocene|Pleistocene|Aeolian sand unit widespread throughout Great Victoria Desert (Benbow, 1986,1993; Benbow et al, 1995b) believed to form base of dunefield and core of dunes on OOLDEA. Excellent exposures in sections through dunes and swales are along railway line to the east. Thickness: at least 10 m. Age inferred. Source of sand includes Hampton Formation and Ooldea Sand. A pervasive and extensive calcrete has developed on and within this unit. |||||Aeolian; dominantly red-brown to orange-brown sand (partly clayey, particularly in swales; moderately good sorting; v.fine-medium sand); coarse-v.coarse grained, rounded, quartz sand component forming lag on surface; distinctive carbonate palaeosols.|
27617|Wipajiri Formation|23770|5|Briefly described|p1|Tertiary|Tertiary|Formerly known as Wipajiri Channel Sand.||||||
27617|Wipajiri Formation|29673|6|Mentioned|p317|||||||||
27617|Wipajiri Formation|30056|6|Mentioned|p140|||||||||
27617|Wipajiri Formation|30163|6|Mentioned|p653|||||||||
27617|Wipajiri Formation|30804|5|Briefly described|p13|||On Table 1||||||
27617|Wipajiri Formation|30807|6|Mentioned|p101|||Suggested map symbol||||||
27617|Wipajiri Formation|30919|6|Mentioned|Map legend|Pliocene|Pliocene|Prob. Pliocene||||||
27617|Wipajiri Formation|32652|6|Mentioned|Table 2|||||||||
27617|Wipajiri Formation|33824|6|Mentioned|Table 2|||||||||
27617|Wipajiri Formation|37678|6|Mentioned|p238|||||||||
27617|Wipajiri Formation|40754|6|Mentioned|p11|||||||||
27617|Wipajiri Formation|40755|5|Briefly described|p43|||||||||
27617|Wipajiri Formation|40756|5|Briefly described|p3|||||||||
27617|Wipajiri Formation|40757|3|Fully described|p81|||Mention p76.||||||03-SEP-18
27617|Wipajiri Formation|40758|6|Mentioned|p88|||||||||
27617|Wipajiri Formation|41537|6|Mentioned|p349|||||||||
27617|Wipajiri Formation|42375|5|Briefly described|p39-29|||Lake Eyre Basin Defined Stirton 1961.||||||
27617|Wipajiri Formation|43041|5|Briefly described|Fig.1,p590|||||||||
27617|Wipajiri Formation|44133|5|Briefly described|p194, 190 Fiig. 10.30|Late Miocene|Middle Miocene|Geoloigcal Province: Lake Eyre Basin. Thickness: 1m. ||||||
27617|Wipajiri Formation|44223|14|Not recorded|p.159|||Ref. to Stirton, Telford et al., 1966.||||||
27617|Wipajiri Formation|44238|14|Not recorded|p.225,227||Miocene|Fig.3.||||||
27617|Wipajiri Formation|45128|6|Mentioned|p54|||||||||
27617|Wipajiri Formation|45145|6|Mentioned|Table 7|||||||||
27617|Wipajiri Formation|46902|6|Mentioned|Table 1|||Correlation chart for Cainozoic land-surfaces||||||
27617|Wipajiri Formation|60703|5|Briefly described|p704 Fig. 2, p725 Fig. 18|Early Miocene|Early Miocene|Contains fossils of teleost fish and bivalves. Overlies the Etadunna Formation. Age: ca 24 Ma based on paleomag. is at odds with younger age determined from palynology (p732). Geological Province: Lake Eyre Basin.||||||06-SEP-10
27617|Wipajiri Formation|61119|5|Briefly described|p124, p137, pp143-144, p146||Cenozoic|Younger than Etadunna Formation [overlies]. Freshwater channel deposits 'intruding' [deposited in weathered top of] Etadunna Formation. Detailed descriptions of Lungfish fossil assemblages included.||||||28-MAR-12
27617|Wipajiri Formation|61155|5|Briefly described|p17|Middle Miocene|Middle Miocene|Age: 11.5-10.5Ma. Geological Province: Lake Eyre Basin.||||||
27617|Wipajiri Formation|66131|5|Briefly described|p240, p242 Fig.2, p245-246, p256|Miocene|Miocene|Defined by Stirton et al. (1967) from Lake Ngapakaldi. Contains vertebrate remains and Unionid shell impressions. Probably includes the (unnamed) black clay and white sand underlying Tirari Formation at Lake Hydra, which are interpreted as a meandering fluvial system or a lacustrine delta-fan. ||||Overlain by the Tirari Formation.|Consists of coarser conglomeratic lenses; may be a channel fill within Etadunna Formation.|
27617|Wipajiri Formation|66573|5|Briefly described|p874, p875 Tb.2|Miocene|Miocene|Contains Kutjamarpu local fauna. Fills paleochannels incised into top of Etadunna Formation. White quartz sand and grey shale. c.16 Ma.||||||
27617|Wipajiri Formation|67462|5|Briefly described|Map legend.|Miocene|Miocene|Tirari Sub-basin, Lake Eyre Basin.||||||
27617|Wipajiri Formation|68715|6|Mentioned|p30 Fig.5|Tortonian|Serravallian|Tirai and northern Callabonna sub basins, Lake Eyre Basin.||||||
27617|Wipajiri Formation|69019|5|Briefly described|p105 Fig.25.|Miocene|Miocene|Tirari Sub-basin.||||Overlies Etadunna Formation.||
27617|Wipajiri Formation|69023|6|Mentioned|p108|Miocene|Miocene|Tirari Sub-basin, Lake Eyre Basin.||||||
35880|Wiperaminga Subgroup|23347|2|Defined|p51 Tb. 1, p52|Statherian|Statherian|Lowest unit of Curnamona Group (Willyama Supergroup). Modified from "Wiperaminga group" of CEC and Esso Minerals. Age: 1715+/-3Ma and 1712+/-2Ma. Underlies Ethiudna Subgroup. Dominated by interlayered albitised and schistose metasediments. More detail inc||||||24-MAR-09
35880|Wiperaminga Subgroup|23476|5|Briefly described|p50|||||||||
35880|Wiperaminga Subgroup|24289|5|Briefly described|p46|Paleoproterozoic|Paleoproterozoic|Of Curnamona Group.||||||07-NOV-08
35880|Wiperaminga Subgroup|24431|5|Briefly described|p189 Fig. 1|||Of the Curnamona Group. Conformably overlain by the Ethiudina Subgroup. Geological Province: Olary Domain.||||||
35880|Wiperaminga Subgroup|24582|5|Briefly described|p4|Paleoproterozoic|Paleoproterozoic|Biotite-quartzofeldspathic gneiss. Hosts Au deposits. In the Olary Block. Geological Province: Curnamona Province.||||||07-NOV-08
35880|Wiperaminga Subgroup|60485|5|Briefly described|p28 Fig. 2|||Of the Curnamona Group. Geological Province: Olary Domain.||||||
35880|Wiperaminga Subgroup|61032|5|Briefly described|p6|Paleoproterozoic|Paleoproterozoic|Of the Willyama Supergroup. Biotite-quartzofeldspathic gneiss, hosting Au mineralisation.||||||07-NOV-08
35880|Wiperaminga Subgroup|61734|5|Briefly described|p52 Fig.2|Statherian|Statherian||1.71 Ga|Of the Curnamona Group.||Is overlain by Ethiudna Subgroup. Is intruded by Basso and Lady Louise Suites.|Dominated by albitised and schistose metasediments.|
35880|Wiperaminga Subgroup|61736|5|Briefly described|p666 Fig. 3|Paleoproterozoic|Paleoproterozoic|Of Curnamona Group. Age: </-1716+/-6Ma. Geological province: Olary Domain.||||||
35880|Wiperaminga Subgroup|62373|5|Briefly described|p503|Paleoproterozoic|Paleoproterozoic|Of the Curnamona Group (Willyama Supergroup). Migmatiseed, quartz-feldspathic rocks and albite-quartz rocks. Geological Province: Curnamona Province/Olary Domain.||||||07-NOV-08
35880|Wiperaminga Subgroup|62514|5|Briefly described|p748 Fig. 3|Mesoproterozoic|Mesoproterozoic|Of the Curnamona Group. Intruded by Basso Suite  rocks.  Age: <1700Ma. Geological Province: Olary Domain/Curnamona Province||||||16-SEP-09
35880|Wiperaminga Subgroup|62535|5|Briefly described|p666 Fig.3, p670, p672|Paleoproterozoic|Paleoproterozoic|Olary Domain.||Curnamona Group.||Is overlain by Ethiudna Subgroup. Interbedded with Basso Suite.|Extensively albitized psammopelite-psammite-pelite succession. Includes volcanic units.|
35880|Wiperaminga Subgroup|62592|5|Briefly described|p16 Fig.2.2. |||Olary Domain, Curnamona Province.||Lower unit in Curnamona Group.||Is intruded by Basso Suite.||
35880|Wiperaminga Subgroup|62993|5|Briefly described|p8, p10, p11, 12, 16, p37, 40, 42|Paleoproterozoic|Paleoproterozoic|Olary Domain.||Curnamona Group|Includes George Mine Formation, Mooleugore Formation, Tommie Wattie Formation||Includes quartzofeldspathic gneiss.|19-DEC-21
35880|Wiperaminga Subgroup|63102|4|Described|p13-15,18-20,30,34-35,37,57-60|Statherian|Statherian|Geological province: Olary Domain, Curnamona Province. Outcrops extensively in the Olary Domain. Includes informal nomenclature used by Esso Australia e.g. 'D' (lower schist formation), 'L' (lower albite horizon) and 'M' (middle schist). Hosts significant Cu-Au mineralisation, preferentially occuring at the contact between Ethiudna and Wiperaminga subgroups. Shows stratiform mineralisation; iron formations (commonly baritic) with local Cu and Au in the upper part of the subgroup. Also shows stratabound mineralisation; disseminated sediment-hosted Fe, Cu, Zn, Co, W, U, F.||Unit of Curnamona Group.|Includes Tommie Wattie Formation and Mooleugore Formation and George Mine Formation.|Overlain by Ethiudna Subgroup.|Quartzofeldspathic rocks, schistose metasediments and migmatites.|
35880|Wiperaminga Subgroup|63186|5|Briefly described|p66, p67|Paleoproterozoic|Paleoproterozoic|Of the Curnamona Group (Willyama Supergroup). Calc-silicate rocks - dominate in the Olary Domain of the Curnamona Province.||||||07-NOV-08
35880|Wiperaminga Subgroup|63866|5|Briefly described|p40|||Olary Domain, Curnamona Province.||Curnamona Group||Overlain by the Ethiudna Subgroup.|Pelite, psammopelite, psammite, albite granofels interlayered with migmatitic schist, magnetite-rich units and volcaniclastic units.|
35880|Wiperaminga Subgroup|64741|4|Described|p301 Fig. 4, p302|Paleoproterozoic|Paleoproterozoic|Of Curnamona Gp. Includes George Mine + Tommie Wattie Fms. Geol.province: Olary Domain. Oldest known lithostratigraphic unit of Willyama Supergroup. Dominantly clastic with the only chemical sediments being quartz-rich, containing iron; some brecciation||||||07-FEB-11
35880|Wiperaminga Subgroup|64742|5|Briefly described|p321 Fig.3, pp325-327.|||Major and trace element analyses, and Sm-Nd isotope data, are detailed.||Unit in Curnamona Group.||Is overlain by Ethiudna Subgroup.|Albitite, albitic psammite, plagioclase-quartz-mica schist, quartzite.|29-MAR-12
35880|Wiperaminga Subgroup|64744|5|Briefly described|p353 Fig.4, p354. |Statherian|Statherian|Olary Domain.||Unit in Willyama Supergroup.||Is overlain by Ethiudna Subgroup.|Psammopelitic schists and gneisses.|
35880|Wiperaminga Subgroup|64944|5|Briefly described|p27, p28 Fig. 1, p29 Tb. 1|Paleoproterozoic|Paleoproterozoic|Lower part of Curnamona Group.Contains Mooleugore, Tommie Wattie and George Mine Formations. Underlies the Ethiudna Subgroup. Age: 1719-~1711.5Ma. Geol. province: Olary Domain. Essentially equivalent to "Quartzofeldspathic Suite" of Clarke et al (1986)||||||07-FEB-11
35880|Wiperaminga Subgroup|65407|6|Mentioned|p239 Fig.3|||||Curnamona Group.|||Quartz-magnetite albitite.|
35880|Wiperaminga Subgroup|66302|5|Briefly described|p36 Fig.9, p37, p39|Statherian|Statherian|Olary Domain, Curnamona Province. |ca. 1718 Ma|Curnamona Group|Includes the George Mine Formation, Mooleughore Formation and Tommie Wattie Formation.|Overlain by the Ethiudna Subgroup.||
35880|Wiperaminga Subgroup|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Olary Domain.|1716 +/- 6 Ma (maximum depositional age).|Curnamona Group.||Is intruded by Basso Suite and Poodla Hill Granite.||
35880|Wiperaminga Subgroup|69213|5|Briefly described|p34, p35 Fig. 11|Paleoproterozoic|Paleoproterozoic|Olary Domain, Curnamona Province. ||Curnamona Group, Willyama Supergroup. ||Ethiudna Subgroup overlies.|Migmatites with albitic leucosomes. Migmatites range from transitional metatexite to diatexite.|
35880|Wiperaminga Subgroup|70405|4|Described|p9 table 1, p15, p16, p43 Table 3, |Paleoproterozoic|Paleoproterozoic||1710 Ma-1720 Ma|Curnamona Group|Includes George Mine Formation|Underlies Ethiunda Subgroup, intruded by Lady Louise Suite|Migmatites and granites with albite rich leucosomes. Granites are medium-coarse grained and grade to pegmatites.|
35880|Wiperaminga Subgroup|70657|4|Described|p12, p13 Fig.6, p14-15, p17-18, p21|Statherian|Statherian|See also p23-26, p29, p31, p60, p63-66. This name was modified by Conor (2000) from one of several informal schemes of Esso. Stratigraphy is imperfectly defined. Curnamona Province; Olary Domain. No equivalent in Broken Hill Domain. The base has not yet been recognised. Mineralisation described in some detail. Na-alteration mentioned.|~1718 Ma|Curnamona Group|Mooleugore, Tommie Wattie, George Mine Formations; Morialpa Migmatite.|Interbedded with Basso Suite flows. Underlies Ethiudna Subgroup (Cathedral Rock Formation). No equivalent in Broken Hill Domain. Intruded by Lady Louise Suite.|Interlayered quartzofeldspathic rocks, albite granofels (i.e. albitite), schistose metasediments, composite gneiss and migmatite. A-type metagranitoids and metavolcanics enriched in U and Th.|
35880|Wiperaminga Subgroup|70658|5|Briefly described|p5-6, 9-10, 15|Paleoproterozoic|Paleoproterozoic|Olary Domain, Curnamona Province.||Curnamona Group.|George Mine Formation.|Is overlain by Ethiudna Subgroup.|Interlayered granofels and composite gneiss.|
35880|Wiperaminga Subgroup|72461|6|Mentioned|p6||||c. 1730 Ma|||||19-DEC-21
35880|Wiperaminga Subgroup|73429|5|Briefly described|p106 Fig.2, p107|Statherian|Statherian|Curnamona Province, Olary Domain.||base of Curnamona Group||Underlies Ethiudna Subgroup|Migmatised, quartz-feldspathic and albite-quartz rocks.|
79805|Wire Dam Dolerite|71037|4|Described|p20, p22-23 Fig.2, p24, p26, p27 Fig.6|Paleoproterozoic|Paleoproterozoic|These rocks previously included in Broadview Schist. See also p27.  Forms sills up to 50 m thick of variably foliated, epidote-altered, fine to coarse-grained, equigranular, dark green dolerite (Fig. 3a) to gabbro, with minor basalt. Maximum age from Broadview Schist. Minimum age from Tip Top Granite, believed to have been intruded at the time of foliation/deformation.|c. 1795-1775 Ma.|||Intrudes Broadview Schist metasediments as sills. Older than Tip Top Granite.|Dolerite, thinner units finer grained and thicker units with gabbroic cores and doleritic chilled margins. Increasingly metamorphosed to amphibolite and foliated metabasalt to the south.|
79805|Wire Dam Dolerite|71129|2|Defined|p1,3,25-27,104,155,183-184|Statherian|Statherian|Geological Province: Gawler Craton. Name derived from Wire Dam on Pandurra Station.Type locality: SA Geodata Field Observation site 2012588, located at GDA 94, zone 53 715880mE, 6385409mN (2.6 km SE of Wire Dam on Pandurra Station). Minor mafic sills hosted within the Broadview Schist, dolerite sheets aligned sub-parallel to bedding. Thickness of individual sheets up to 50m. Variably foliated with epidote alteration, and locally form thinner sheets of very fine- to fine-grained, well foliated (more highly strained) meta-basalts. Has previously been mapped as a sub-unit of broadview Schist, but has since been described as a distinct geological unit based on unlikely petrogenetic relationships between the dolerites and metasedimentary host rocks. Widespread unit in SW SIX MILE HILL, bounded to the east by N-striking Roopena Fault and south of Gawler Range Volcanics. Shows similar foliation to that of the Broadview Schist host rock and the intrusive Tip Top Granite, indicating sill emplacement to pre-date c. 1775 Ma deformation event. See also p189-194,197-198,204-205,225,227-228,230.|Between c. 1795 to c. 1775 Ma|Of the Wire Dam Suite.||Intrudes the Broadview Schist.|Sills of fine- to coarse grained, equigranular, dark green dolerite to gabbro; weakly to very well-developed foliation and a locally developed lineation. Elsewhere consists of fine-grained, equigranular, well foliated meta-basalts and amphibolites.|13-NOV-19
79805|Wire Dam Dolerite|71130|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic||c.1790-1775 Ma.|||Intrudes Broadview Schist.|Dolerite, thinner units finer-grained and thicker units with gabbroic cores and doleritic chilled margins. Increasingly metamorphosed to amphibolite and foliated merabasalt to the south.|
79805|Wire Dam Dolerite|71131|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic||c.1790-1775 Ma.|||Intrudes Broadview Schist.|Dolerite, thinner units finer-grained and thicker units with gabbroic cores and doleritic chilled margins. Increasingly metamorphosed to amphibolite and foliated merabasalt to the south.|
79805|Wire Dam Dolerite|71414|6|Mentioned|p42 Fig 1|Statherian|Statherian|Geological province: Gawler Craton.|~1770 Ma|||Intrudes Broadview Schist.||
79805|Wire Dam Dolerite|72089|6|Mentioned|p3|Palaeoproterozoic|Palaeoproterozoic|Gawler Craton.||||||
79805|Wire Dam Dolerite|72237|6|Mentioned|p29|Paleoproterozoic|Paleoproterozoic|Geological province: Gawler Craton.||||||
79805|Wire Dam Dolerite|73103|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic||~1790 - 1775 Ma.|||Intrudes Broadview Schist (as sills).|Dolerite, thinner units finer-grained and thicker units with gabbro cores and doleritic chilled margins. Increasingly metamorphosed to amphibolite and foliated metabasalt to the south.|
79805|Wire Dam Dolerite|73110|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic||~1790 - 1775 Ma.|||Intrudes (as sills) Broadview Schist.|Dolerite, thinner units finer grained and thicker units with gabbroic cores and doleritic chilled margins. Increasingly metamorphosed to amphibolite and foliated metabasalt to the south.|
79805|Wire Dam Dolerite|73162|6|Mentioned|p452 Fig.3|Paleoproterozoic|Paleoproterozoic|||||||
29947|Wirrda Subsuite|22430|6|Mentioned|p2||Proterozoic|||||||
29947|Wirrda Subsuite|43052|5|Briefly described|p128 Table 5.6|||Hiltaba Suite. Various dates given between 1613+/-20 and 1590 +/-5 Ma, but unclear what was dated.|||||Bimodal suite of medium-grained and porphyritic rock types including quartz monzodiorite, quartz monzonite, syenite, aplite|13-SEP-12
29947|Wirrda Subsuite|65390|5|Briefly described|p26 Tb. 1|Calymmian|Calymmian|Of Hiltaba Suite. Olympic Dam. Bimodal suite of medium-grained and porphyritic rock types including quartz monzodiorite, quartz monzonite, syenite and aplite. Various ages listed; most recent (U-Pb zircon, measured in 1993) range from 1598 +/- 2 to 1590 +5/-4 Ma.||||||
29947|Wirrda Subsuite|72065|6|Mentioned|p112|||Geological province: Olympic Province, Gawler Craton. Contains 'HS-type' crystal clusters: fine- to medium-grained magnetite-apatite+\-titanite+\-biotite-chlorite+\-zircon. (HS: Hiltaba Suite type).||||||
26332|Wirriecurrie Granite|22629|6|Mentioned|p156|Statherian|Statherian|Age: 1793+/-8Ma||||||
26332|Wirriecurrie Granite|23054|5|Briefly described|p8-10,32-3||Statherian|Max Age: 1793 (+/-) 8 Ma.||||||
26332|Wirriecurrie Granite|23480|5|Briefly described|p20, 21|Proterozoic|Proterozoic|||||||
26332|Wirriecurrie Granite|24197|5|Briefly described|p75 Tb. 8.1|Paleoproterozoic|Paleoproterozoic|Age: 1793Ma.||||||07-FEB-11
26332|Wirriecurrie Granite|24506|5|Briefly described|p16|||Age: 1793+/-8Ma.  Intrudes Peake Metamorphics.  Geological Province: Peake and Denison Inliers.||||||18-JAN-07
26332|Wirriecurrie Granite|24526|5|Briefly described|p100|Paleoproterozoic|Paleoproterozoic|Syn-tectonic rocks.  Age: 1793+/-8Ma.||||||07-NOV-08
26332|Wirriecurrie Granite|36733|2|Defined|p71|Mesoproterozoic|Mesoproterozoic|See also p14,21.||||||18-JAN-07
26332|Wirriecurrie Granite|38108|6|Mentioned|Table 1|||||||||
26332|Wirriecurrie Granite|41972|6|Mentioned|p374|||||||||
26332|Wirriecurrie Granite|43052|4|Described|p101|||Minimum age of 1648+/-21 Ma.||||||18-JAN-07
26332|Wirriecurrie Granite|43053|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Peake Inlier and Denison Inlier.||||||07-NOV-08
26332|Wirriecurrie Granite|43258|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
26332|Wirriecurrie Granite|43298|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
26332|Wirriecurrie Granite|44289|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
26332|Wirriecurrie Granite|50605|5|Briefly described|p(iii), 11.3|Paleoproterozoic|Paleoproterozoic|Geological Province: Gawler Craton and Curnamona Province. Age: 1648 +/- 21Ma (Rb-Sr), 1793 +/- 8Ma (SHRIMP).||||||04-MAR-13
26332|Wirriecurrie Granite|60953|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Age: 1793Ma. Porphyritic to gneissic granitoids.||||||07-NOV-08
26332|Wirriecurrie Granite|61108|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|Porphyritic to gneissic granite, adamellite and granodiorite. Age: 1793 Ma.||||||07-NOV-08
26332|Wirriecurrie Granite|61262|5|Briefly described|p455 Fig. 11|Paleoproterozoic|Paleoproterozoic|Age: ~1800Ma. Geological Province: northern Gawler Craton.||||||07-NOV-08
26332|Wirriecurrie Granite|64725|6|Mentioned|p58 Fig.2. |||Gawler Craton.||||||
26332|Wirriecurrie Granite|64726|6|Mentioned|p83 Fig.2.|||||||||
26332|Wirriecurrie Granite|65376|5|Briefly described|pp237-238.||||1787 +/- 8 Ma.|||Sheared against Peake Metamorphics to the south.|Augen gneiss, granitic gneiss, foliated porphyritic granite, adamellite, granodiorite and aplite.|
26332|Wirriecurrie Granite|65390|5|Briefly described|p13, p22 Fig. 3|Statherian|Statherian|Syn-tectonic with Peake Metamorphics. Age of 1780 Ma given.||||||
26332|Wirriecurrie Granite|66302|5|Briefly described|p30|Statherian|Statherian||1787 +/- 8 Ma (Fanning et al, 2007)|||Faulted against the Peake Metamorphics.|Granite and augen gneiss.|
26332|Wirriecurrie Granite|67323|5|Briefly described|p31|||Gawler Craton.|~1775 Ma.|||||
26332|Wirriecurrie Granite|67536|5|Briefly described|Map Legend|Statherian|Orosirian|Gawler Craton.|1793 +/- 8 Ma||||Granite, adamellite, granodiorite.|
26332|Wirriecurrie Granite|69203|5|Briefly described|p34|||Peake and Denison Inlier, northern Gawler Craton. Associated with the Tidnamurkana Volcanics.|1787 +/- 8 Ma.|||||
26332|Wirriecurrie Granite|69554|6|Mentioned|p135|||Peake and Denison Domain, northern Gawler Craton. Associated with Tidnamurkana Volcanics.|1787 +/- 8 Ma.|||||
26332|Wirriecurrie Granite|70938|5|Briefly described|p807-808|Paleoproterozoic|Paleoproterozoic|Denison Range. Deformed towards its margins: causal events debated. Deformation interpreted to be related to the Musgravian and Delamerian Orogenies.|1793 +/- 8 Ma; Rogers and Freeman (1994).|||||13-DEC-19
26332|Wirriecurrie Granite|71318|5|Briefly described|p3,19-20|Paleoproterozoic|Paleoproterozoic|Geological province: Gawler Craton. Occurs in the Peak and Denison Inlier of the NE Gawler Craton. Sample GSSA 2017962 (weakly metamorphosed granite) yielded an interpreted (weighted mean 207Pb/206Pb age) magmatic crystallisation age of 1770+\-13 Ma.||||Southern border in sheared contact with Peake Metamorphics.|Augen gneiss, granitic gneiss, foliated porphyritic granite, adamellite, granodiorite and aplite.|
26332|Wirriecurrie Granite|71348|5|Briefly described|p200|Statherian|Statherian|Broadly coeval with Tidnamurkuna Volcanics.|1787+\-8 Ma|||||
26332|Wirriecurrie Granite|73155|6|Mentioned|p281|Statherian|Statherian|Gawler Craton.|ca. 1790 Ma|||||
24581|Wisanger Basalt|22458|5|Briefly described|p523, Fig.1 p524||Jurassic|||||||
24581|Wisanger Basalt|38008|2|Defined|p1|Jurassic|Jurassic|||||||
24581|Wisanger Basalt|38699|6|Mentioned|p12|||||||||
24581|Wisanger Basalt|39842|6|Mentioned|p5|||||||||
24581|Wisanger Basalt|41218|6|Mentioned|p324|||||||||
24581|Wisanger Basalt|41513|6|Mentioned|p35|||||||||
24581|Wisanger Basalt|42361|5|Briefly described|p4|||Found on Kangaroo Island||||||
24581|Wisanger Basalt|42899|5|Briefly described|p347|||||||||
24581|Wisanger Basalt|42900|5|Briefly described|p395|||||||||
24581|Wisanger Basalt|43026|5|Briefly described|p585|||||||||
24581|Wisanger Basalt|43053|5|Briefly described|Map Legend|Jurassic|Jurassic|||||||25-MAY-05
24581|Wisanger Basalt|43195|6|Mentioned|Map Commentary||Middle Jurassic|||||||
24581|Wisanger Basalt|43258|5|Briefly described|Map Legend||Jurassic|||||||
24581|Wisanger Basalt|43298|5|Briefly described|Map Legend||Jurassic|||||||
24581|Wisanger Basalt|44133|5|Briefly described|p68, 149, 94 Fig. 9.2|Jurassic|Jurassic|Overlies Cape Jervis Formation. Thickness: 30m. Age: ~170Ma.||||||13-SEP-18
24581|Wisanger Basalt|60953|5|Briefly described|Map Legend|Jurassic|Jurassic|||||||
24581|Wisanger Basalt|61108|5|Briefly described|map legend|Jurassic|Jurassic|||||||
24581|Wisanger Basalt|63124|5|Briefly described|p57|Middle Jurassic|Middle Jurassic|Basalt flow remnant on Kangaroo Island. ||||||
24581|Wisanger Basalt|64282|5|Briefly described|Map legend|Jurassic|Jurassic|Geolocial Province: ?Eucla Basin. Dark, fine-grained basalt up to 15m thick with pillows, columnar jointing and quartz-filled vesicles.||||||22-DEC-21
24581|Wisanger Basalt|64570|5|Briefly described|p861|Mesozoic|Mesozoic|Found on Kangaroo Island, SA. See also misspelling Winsanger Basalt, p859.||||||30-JAN-09
24581|Wisanger Basalt|65375|6|Mentioned|p49.|Jurassic|Jurassic|Kangaroo Island.  Evidence of further separation of Australia and Antarctica.||||||
24581|Wisanger Basalt|65376|6|Mentioned|p9 Fig.1.2. |Jurassic|Jurassic|||||||
24581|Wisanger Basalt|65921|6|Mentioned|p2 (map legend)|Jurassic|Jurassic|Maximum age is Upper Triassic.||||||
24581|Wisanger Basalt|68131|5|Briefly described|p2 Fig.1|Jurassic|Jurassic|Kangaroo Island.|||||Basalt.|
24581|Wisanger Basalt|69372|6|Mentioned|p26, p28, fig. 6, p29-30, 32, 33, 34,38|Jurassic|Jurassic||179 Ma-169 Ma|||Overlies Cape Jervis Formation.|Basalt.|18-JAN-17
24581|Wisanger Basalt|69878|5|Briefly described|p404-405|Jurassic|Jurassic|Kangaroo Island. Lava flows with geochemical and isotopic signatures virtually identical to the chilled margins of Tasmanian dolerite. Represents an outlier of the Ferrar Magmatic Province.||||||
24581|Wisanger Basalt|70660|5|Briefly described|p40|Jurassic|Jurassic|||||||
24581|Wisanger Basalt|73107|5|Briefly described|Map legend.|Jurassic|Jurassic||||||Dark, fine-grained basalt up to 15m thick with pillows, columnar jointing and quartz-filled vesicles.|
24581|Wisanger Basalt|73129|6|Mentioned|p47 Fig.6|||Described with lamprophyric intrusives.||||||09-JUN-22
39170|Wokurna Member|24475|2|Defined|p52|Paleoproterozoic|Paleoproterozoic|Of Wandearah Formation. Overies Delken Member and New Cornwall Member. Intruded by Bute Metadolerite.  Includes Ninnes Member of Zang (2002).||||||07-NOV-08
39170|Wokurna Member|65375|5|Briefly described|p19, p21.|Paleoproterozoic|Paleoproterozoic|Equivalent to the former Wandearah Metasiltstone.||Unit in Wandearah Formation.||Overlies Doora Member. Is intercalated with Willamulka Metabasalt Member.|Red-brown siltstone, calc-silicate and albitic rocks.|
39170|Wokurna Member|65376|5|Briefly described|p101, p106, p109.|||Age interpreted from age of intercalated Mona Volcanics Member sample.|1735 +/- 10 Ma.|Unit in Wandearah Formation.||Intercalated with the Mona Volcanics Member in the Bute region.||
68099|Woman-in-White Amphibolite|60485|5|Briefly described|p28 Fig. 2|Statherian|Statherian|Of the Lady Louise Group.  Age: 1685+/-4Ma (conflicts with Calymmian info???).  Geological Province: Olary Domain. Intrusive rocks.||||||28-APR-05
68099|Woman-in-White Amphibolite|62373|5|Briefly described|p508|Paleoproterozoic|Paleoproterozoic|Of the Lady Louise Suite. Age: 1685 Ma (SHRIMP U-Pb)||||||07-NOV-08
68099|Woman-in-White Amphibolite|62592|5|Briefly described|p16 Fig.2.2. |Statherian|Statherian|Olary Domain, Curnamona Province.|1685 +/- 4 Ma.|||||
68099|Woman-in-White Amphibolite|62993|5|Briefly described|p7|Paleoproterozoic|Paleoproterozoic||1685 Ma (SHRIMP)|Lady Louise Suite|||Dominantly mafic sill locally differentiated into amphibole granite.|
68099|Woman-in-White Amphibolite|63102|5|Briefly described|p12-13,31,35,40-41|||Geological province: Olary Domain, Curnamona Province. Nomenclature after Conor and Fanning (2001). Equivalent to a 'soda-rich composite intrusive stock' (Segnit 1949).|1685+\-4 Ma|Unit of Lady Louise Suite.||Intrudes Abminga Subsuite.|Differentiated sills; amphibole, plagioclase and epidote, but commonly includes minor quartz, opaques, titanite and traces of sulphide (including chalcopyrite).|
68099|Woman-in-White Amphibolite|63866|5|Briefly described|p41||||1685 +/- 4 Ma (Conor and Fanning, 2001)|||||
68099|Woman-in-White Amphibolite|66302|6|Mentioned|p38|Statherian|Statherian|Olary Domain, Curnamona Province. |1685 +/- 4 Ma (Conor and Fanning, 2001)|Lady Louise Suite||||
68099|Woman-in-White Amphibolite|66526|5|Briefly described|p36.|Proterozoic|Proterozoic|Curnamona Province. Has widespread correlatives in Central Gawler, Warumpi, Aileron, Mount Isa and Georgetown Provinces. Produced in the Woman-in-White Event, ME 13 in the Proterozoic Mafic-Ultramafic Magmatic Event Series.|c.1680 Ma.|||||
68099|Woman-in-White Amphibolite|70657|4|Described|p12, p31, p47-48|Statherian|Statherian|Conor and Fanning (2001). Occurs in the western limb of the major fold at Mulga Bore Creek. Curnamona Province; Olary Domain. |1685 +/- 4 Ma (Conor and Fanning, 2001).|Lady Louise Suite||Equivalent to Parnell Formation. Intrudes Abminga Subsuite, Ethiudna Subgroup.|Dominantly amphibole, plagioclase and epidote; commonly includes minor quartz, opaques, titanite and traces of sulfide (including chalcopyrite). Metamorphosed.|
68099|Woman-in-White Amphibolite|70658|6|Mentioned|p32|||Curnamona Province.||Lady Louise Suite.|||A large differentiated granite sill.|
29166|Wongo Pedoderm|31532|3|Fully described|Table 1|||||||||
25645|Wonoka Formation|7931|4|Described|p97-99|Ediacaran|Ediacaran|Of Wilpena Group. Gradationally overlain by Bonney Sandstone + Rawnsley Quartzite (=Pound Subgroup). Geol.Prov: Adelaide Geosyncline. Upper and lower Wonoka Formations mentioned. Dominated by marine limestone, calcareous mudstone and sandstone.||||||07-FEB-11
25645|Wonoka Formation|9862|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Probably of the Wilpena Group. Laminated grey calcareous siltstone, minor carbonate.||||||
25645|Wonoka Formation|22646|6|Mentioned|Fig 4 on p 102|Neoproterozoic|Neoproterozoic|Adelaide Geosyncline (West).  Age - Ediacarian in text.||||||
25645|Wonoka Formation|22746|5|Briefly described|p527, p528|||See also Table 1 p524||||||
25645|Wonoka Formation|22772|5|Briefly described|Table13.1|Neoproterozoic III|Neoproterozoic III|||||||
25645|Wonoka Formation|22802|6|Mentioned|p872|||Adelaide Geosyncline||||||
25645|Wonoka Formation|22857|5|Briefly described|Tb. 13.1 (insert p70-71)|Marinoan|Marinoan|Of the Wilpena Group. ||||||
25645|Wonoka Formation|22921|6|Mentioned|37|||||||||
25645|Wonoka Formation|22927|5|Briefly described|40|||Geol province Adelaide Geosyncline. Underlying unit Bunyeroo Formation||||||
25645|Wonoka Formation|23178|6|Mentioned|p30, Fig.1||Neoproterozoic|Parent: Wilpena Group||||||
25645|Wonoka Formation|23180|6|Mentioned|p36, Fig.1|||Age: Adelaidean||||||
25645|Wonoka Formation|23211|6|Mentioned|p44, Fig.2|||of Depot Springs Subgroup.||||||
25645|Wonoka Formation|23250|5|Briefly described|p1124 Fig.2||Neoproterozoic III|of Wilpena Group. Correlate of Julie Formation.||||||
25645|Wonoka Formation|23282|6|Mentioned|p93|||||||||
25645|Wonoka Formation|23287|6|Mentioned|Fig.2-4|||Age: Upper Ediacarian. of Adelaide Geosyncline.||||||
25645|Wonoka Formation|23288|6|Mentioned|Fig.5|||||||||
25645|Wonoka Formation|23314|5|Briefly described|331 Fig.2|||||||||
25645|Wonoka Formation|23315|5|Briefly described|p345|Neoproterozoic|Neoproterozoic|Of the Wilpena Group.  Shale, siltstone and dolomite.||||||07-FEB-07
25645|Wonoka Formation|23394|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of Wilpena Group||||||
25645|Wonoka Formation|23401|5|Briefly described|p573|||Underlying unit Bunyeroo Formation. Geological Province: Adelaide Fold Belt.||||||
25645|Wonoka Formation|23411|6|Mentioned|Map Legend|||||||||
25645|Wonoka Formation|23445|5|Briefly described|p435|||of Wilpena Group||||||
25645|Wonoka Formation|23562|5|Briefly described|p295 Fig 2|Neoproterozoic III|Neoproterozoic III|||||||
25645|Wonoka Formation|23804|6|Mentioned|p17|||||||||
25645|Wonoka Formation|23806|6|Mentioned|p1122|||||||||
25645|Wonoka Formation|23818|4|Described|p73 Fig.27, p76, 77|Adelaidean|Adelaidean|Of the Wilpena Group. Max. thickness: ~1500 ft. Overlying units: Billy Springs Beds and Pound Quartzite (throughout Flinders Ranges).||||||18-APR-05
25645|Wonoka Formation|23913|4|Described|p108, p110 Fig. 2|Adelaidean|Adelaidean|Geological Province: Central Flinders Zone.  Of the Wilpena Group.  Underlying Unit: Bunyeroo formation.  Overlying Unit: Booney Sandstone.||||||
25645|Wonoka Formation|24175|5|Briefly described|p14|Neoproterozoic|Neoproterozoic|Of the Wilpena Group.  Overlies Bunyeroo Formation.  Max. thickness: >310m.||||||
25645|Wonoka Formation|24176|4|Described|p14, p24 Tb. 1|Adelaidean|Adelaidean|Of the Wilpena Group.  Shales. limestones, calcareous shales, dolomites; stromatolites.  Intertongues with Pound Quartzite and Billy Springs Beds.  Overlies Bunyeroo Formation.  Age is Willouran.  Geological Province: Mount Painter Province.||||||
25645|Wonoka Formation|24195|6|Mentioned|p48|||Geological Province: Angepina Syncline||||||
25645|Wonoka Formation|24321|5|Briefly described|Map legend|Late Adelaidean|Late Adelaidean|Parent: Wilpena Group||||||
25645|Wonoka Formation|24476|4|Described|p547 Fig. 4|Vendian|Vendian|Overlies the Bunyeroo Formation. Overlain by the Bonney Sandstone.  Geological Province: Adelaide fold belt.||||||
25645|Wonoka Formation|24484|5|Briefly described|p803 Fig.3|Neoproterozoic|Neoproterozoic|Overlies the Bunyeroo Formation. Overlain by the Puttapa Conglomerate.||||||
25645|Wonoka Formation|24546|5|Briefly described|p2 - 3 Fig.2|Neoproterozoic|Neoproterozoic|Of Wilpena Group. Geological Province: Adelaide Fold Belt.||||||16-JAN-08
25645|Wonoka Formation|24586|5|Briefly described|p49, p51 Fig. 2, p52 Fig. 3|Adelaidean|Adelaidean|Of the Depot Springs Subgroup (Wilpena Group, Heysen Supergroup. Geological Province: Adelaide Geosyncline. See also p50 Fig. 1 for mention.||||||05-JUL-06
25645|Wonoka Formation|29780|4|Described|p46|||||||||
25645|Wonoka Formation|29781|6|Mentioned|Fig.4|||||||||
25645|Wonoka Formation|30176|6|Mentioned|Map legend|Adelaidean|Adelaidean|Marinoan||||||
25645|Wonoka Formation|30177|4|Described|p91|||||||||
25645|Wonoka Formation|30198|6|Mentioned|p96|||Refers aquifers and lithology on Table 2||||||
25645|Wonoka Formation|30261|6|Mentioned|Table 1|||Marinoan age||||||
25645|Wonoka Formation|30375|6|Mentioned|p205|||||||||
25645|Wonoka Formation|30800|6|Mentioned|Fig.1|||On P220.||||||
25645|Wonoka Formation|30801|6|Mentioned|p5|||Marinoan. Table P5-6||||||
25645|Wonoka Formation|30802|5|Briefly described|p12|||Marinoan||||||
25645|Wonoka Formation|30807|6|Mentioned|p102|||Suggested map symbol||||||
25645|Wonoka Formation|30918|6|Mentioned|p80|||||||||
25645|Wonoka Formation|31388|6|Mentioned|Fig.1|||||||||
25645|Wonoka Formation|31539|6|Mentioned|Fig. 6|||See also Fig. 8, 11, 4, 22.||||||
25645|Wonoka Formation|31730|6|Mentioned|p99|||U.Proterozoic. Geochem. Stream Sediment sampling||||||
25645|Wonoka Formation|31797|6|Mentioned|Fig. 2|||Adelaidean of Wilpena Gp.||||||
25645|Wonoka Formation|31923|6|Mentioned|p10|||||||||
25645|Wonoka Formation|32146|6|Mentioned|Fig.3|||||||||
25645|Wonoka Formation|32419|6|Mentioned|p81|||||||||
25645|Wonoka Formation|32504|6|Mentioned|Fig.2|||||||||
25645|Wonoka Formation|32505|6|Mentioned|Table 3|||||||||
25645|Wonoka Formation|32511|6|Mentioned|Fig.1|||||||||
25645|Wonoka Formation|32720|6|Mentioned|Table 1|||Wilpena Gp.||||||
25645|Wonoka Formation|32722|6|Mentioned|Fig.3|||Adelaidean. Stromatolite||||||
25645|Wonoka Formation|32724|6|Mentioned|Fig.1|||Correlation. Marinoan||||||
25645|Wonoka Formation|32776|6|Mentioned|Fig.2|||||||||
25645|Wonoka Formation|33035|6|Mentioned|p53|||||||||
25645|Wonoka Formation|33036|6|Mentioned|Fig.2|||||||||
25645|Wonoka Formation|33037|6|Mentioned|Fig.2|||||||||
25645|Wonoka Formation|33474|6|Mentioned|Fig.3|||||||||
25645|Wonoka Formation|33655|6|Mentioned|p91|||U. Marinoan. See also P92||||||
25645|Wonoka Formation|33692|6|Mentioned|p162|||See also Fig.3.||||||
25645|Wonoka Formation|34069|6|Mentioned|Fig.2|||||||||
25645|Wonoka Formation|34175|6|Mentioned|p36|||||||||
25645|Wonoka Formation|34267|6|Mentioned|Fig.|||The Oraparinna & Enorama diapiric structures.||||||
25645|Wonoka Formation|34268|6|Mentioned|p241|||U.Prot.||||||
25645|Wonoka Formation|34269|6|Mentioned|Table 1|||||||||
25645|Wonoka Formation|34291|6|Mentioned|p1|||Adelaidean. See also PP18,23,25 etc||||||
25645|Wonoka Formation|34534|6|Mentioned|Fig.2.13|||||||||
25645|Wonoka Formation|34535|4|Described|p76|||See Fig.27||||||
25645|Wonoka Formation|34563|6|Mentioned|p67|||Correlated with Fowlers Gap Beds||||||
25645|Wonoka Formation|34598|6|Mentioned|p22|||||||||
25645|Wonoka Formation|34812|6|Mentioned|p137|||||||||
25645|Wonoka Formation|34835|6|Mentioned|Fig.2|||||||||
25645|Wonoka Formation|34836|6|Mentioned|Fig.2|||||||||
25645|Wonoka Formation|34844|6|Mentioned|p98|||||||||
25645|Wonoka Formation|35075|6|Mentioned|Fig.2|||||||||
25645|Wonoka Formation|35143|6|Mentioned|Fig.2|||||||||
25645|Wonoka Formation|35158|6|Mentioned|p47|||||||||
25645|Wonoka Formation|35195|6|Mentioned|Table 3|||||||||
25645|Wonoka Formation|35217|6|Mentioned|p179|||||||||
25645|Wonoka Formation|35255|6|Mentioned|Fig.6|||See also P15.||||||
25645|Wonoka Formation|35356|6|Mentioned|p30|||||||||
25645|Wonoka Formation|35798|6|Mentioned|Fig.4|||Correlation of lower units in Desert Syncline drill holes.||||||
25645|Wonoka Formation|35863|6|Mentioned|p287|||||||||
25645|Wonoka Formation|36083|5|Briefly described|p472|||||||||
25645|Wonoka Formation|36137|6|Mentioned|p18|||||||||
25645|Wonoka Formation|36622|6|Mentioned|Fig.2|||||||||
25645|Wonoka Formation|36731|6|Mentioned|p122|||Fig.3||||||
25645|Wonoka Formation|36898|6|Mentioned|p197|||||||||
25645|Wonoka Formation|37015|6|Mentioned|Fig.2|||||||||
25645|Wonoka Formation|37461|4|Described|p343|||See also Table 5.I||||||
25645|Wonoka Formation|37627|6|Mentioned|p188|||||||||
25645|Wonoka Formation|37932|6|Mentioned|p547|||||||||
25645|Wonoka Formation|38004|6|Mentioned|p81|||||||||
25645|Wonoka Formation|38022|6|Mentioned|Fig.4|||||||||
25645|Wonoka Formation|38110|6|Mentioned|p3|||||||||
25645|Wonoka Formation|38157|6|Mentioned|Table V|||||||||
25645|Wonoka Formation|38330|6|Mentioned|p217|||||||||
25645|Wonoka Formation|38970|6|Mentioned|Fig.15|||||||||
25645|Wonoka Formation|39210|6|Mentioned|Table 4|||||||||
25645|Wonoka Formation|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Marinoan||||||
25645|Wonoka Formation|39352|6|Mentioned|Map legend|Adelaidean|Adelaidean|Marinoan||||||
25645|Wonoka Formation|39490|6|Mentioned|Fig.1(6)|||||||||
25645|Wonoka Formation|39526|6|Mentioned|p684|||||||||
25645|Wonoka Formation|39675|6|Mentioned|Fig.2|||||||||
25645|Wonoka Formation|39807|6|Mentioned|p225|||||||||
25645|Wonoka Formation|39808|6|Mentioned|p223|||||||||
25645|Wonoka Formation|40455|5|Briefly described|p75|||||||||
25645|Wonoka Formation|40720|5|Briefly described|p55|||||||||
25645|Wonoka Formation|40852|6|Mentioned|Fig.3.2|||||||||
25645|Wonoka Formation|41005|6|Mentioned|p418|||||||||
25645|Wonoka Formation|41236|5|Briefly described|p63|||||||||
25645|Wonoka Formation|41401|6|Mentioned|p33|||||||||
25645|Wonoka Formation|41429|3|Fully described|p233|||||||||
25645|Wonoka Formation|41496|5|Briefly described|Fig.1|||||||||
25645|Wonoka Formation|41500|6|Mentioned|Fig.1|||||||||
25645|Wonoka Formation|41526|6|Mentioned|p27|||||||||
25645|Wonoka Formation|41794|6|Mentioned|p777|||||||||
25645|Wonoka Formation|41801|6|Mentioned|p219|||||||||
25645|Wonoka Formation|41833|6|Mentioned|p586|||||||||
25645|Wonoka Formation|41953|6|Mentioned|Fig.2 P133|||||||||
25645|Wonoka Formation|42028|4|Described|p137|||See also Fig.3 and Fig.4||||||
25645|Wonoka Formation|42095|5|Briefly described|p30|||See also Fig.3||||||
25645|Wonoka Formation|42098|5|Briefly described|p54|||||||||
25645|Wonoka Formation|42222|5|Briefly described|p20|||||||||
25645|Wonoka Formation|42237|6|Mentioned|p98|||||||||
25645|Wonoka Formation|42238|5|Briefly described|Table 1 P74|||||||||
25645|Wonoka Formation|42240|6|Mentioned|Fig.2 P165|||||||||
25645|Wonoka Formation|42241|4|Described|p178|||||||||
25645|Wonoka Formation|42272|5|Briefly described|p404|||||||||
25645|Wonoka Formation|42410|5|Briefly described|p3|||||||||
25645|Wonoka Formation|42546|5|Briefly described|Map legend|Adelaidean (Marinoan)||||||||
25645|Wonoka Formation|42600|5|Briefly described|Table 1 P2|||||||||
25645|Wonoka Formation|42720|5|Briefly described|map legend|Marinoan||||||||
25645|Wonoka Formation|42736|5|Briefly described|map legend|Neoproterozoic||||||||
25645|Wonoka Formation|42813|5|Briefly described|p22|||of Wilpena Group||||||
25645|Wonoka Formation|42882|6|Mentioned|p9|||of Wilpena Group||||||
25645|Wonoka Formation|43052|5|Briefly described|p194,Table 6.1|||of Wilpena Group||||||
25645|Wonoka Formation|43622|5|Briefly described|p39|||||||||
25645|Wonoka Formation|43845|5|Briefly described|Fig3 p43, 42,44,45||Neoproterozoic|In Wilpena Group||||||12-JUL-16
25645|Wonoka Formation|44659|5|Briefly described|map legend|||Marinoan, lithology.||||||
25645|Wonoka Formation|44660|14|Not recorded|map legend|||Marinoan, lithology.||||||
25645|Wonoka Formation|44689|14|Not recorded|map legend|||Andamooka. (H53-12).||||||
25645|Wonoka Formation|46865|6|Mentioned|Table.2|||||||||
25645|Wonoka Formation|50127|6|Mentioned|p48 Fig.2|||Geological Province: Stuart Shelf||||||
25645|Wonoka Formation|60418|5|Briefly described|p134 Fig.1|Neoproterozoic|Neoproterozoic|Of Wilpena Group.||||||
25645|Wonoka Formation|60718|6|Mentioned|p56|||At Patsy Springs.||||||
25645|Wonoka Formation|60889|6|Mentioned|p250 Fig.7|||||||||
25645|Wonoka Formation|60955|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Of the Wilpena Group. Yellow and purple flaggy limestones, green calcareous shales; purple and green siltstones.||||||13-APR-05
25645|Wonoka Formation|60959|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Of the Wilpena Group. Mixed carbonate-siliclastic sequence. Mudstone, calcareous and dolomitic sandstone, limestone, siltstone.||||||
25645|Wonoka Formation|61022|6|Mentioned|p16|||Geological Province: Adelaide Geosyncline. Named in abstract for: The Influence of salt tectonics on Neoproterozoic to Early Palaeozoic sedimentation, Amadeus Basin (abstract) by Dyson, I.A. and Marshall, T.R.||||||20-APR-05
25645|Wonoka Formation|61236|5|Briefly described|p23, p24 Fig. 1|Adelaidean|Adelaidean|Of jenkins (1981).||||||14-MAY-07
25645|Wonoka Formation|61308|5|Briefly described|p7|Proterozoic|Proterozoic|Shale and limestone.||||||
25645|Wonoka Formation|61565|5|Briefly described|p609 Fig. 3|Neoproterozoic III|Neoproterozoic III|Geological Province: Adelaide Fold Belt.||||||26-MAY-06
25645|Wonoka Formation|61732|3|Fully described|p5 Tb. 1, p46-48|Marinoan|Marinoan|Of the Wilpena Group. Includes the basal Wearing Dolomite Member. Overlain by Bonney Sandstone; overlies Bunyeroo Formation. Thick: 700m. Geol P: Adelaide Rift Complex/Stuart Shelf. See also p28 Fig. 13, p151.||||||07-FEB-11
25645|Wonoka Formation|62085|6|Mentioned|p19 Fig.4, p20|Ediacaran|Ediacaran|||Unit in Wilpena Group.|||Siltstone, limestone, sandstone.|
25645|Wonoka Formation|62592|5|Briefly described|p50 Table 5.1.|Ediacaran|Ediacaran|Adelaide Geosyncline.||Unit in Wilpena Group.||Overlies Bunyeroo Formation. Is overlain by Bonney Sandstone.|Limestone, siltstone, sandstone.|
25645|Wonoka Formation|62784|5|Briefly described|p8 Fig.1|Neoproterozoic|Neoproterozoic|Upper unit in Wilpena Group. Overlies Wilcolo Sandstone Member.||||||
25645|Wonoka Formation|62903|6|Mentioned|p730 Fig.1|||Adelaide Rift Complex. Presented in figure as Wonoko.||||overlies Bunyeroo Formation; is overlain by Pound Subgroup||
25645|Wonoka Formation|62962|6|Mentioned|p2296 Tab. 6|||Geological Province: Mount Painter Province. Snadstone and quartzite.||||||07-FEB-11
25645|Wonoka Formation|63458|6|Mentioned|p873, p897 Fig.19.|Ediacaran|Ediacaran|||Unit in Wilpena Group.||Upper part is correlated with Boonall Dolomite.||
25645|Wonoka Formation|63569|6|Mentioned|p118 Fig. 2|Neoproterozoic|Neoproterozoic|||Unit in Wilpena Group.||||
25645|Wonoka Formation|64455|5|Briefly described|p137, p139, p138 Fig. 1|Ediacaran|Ediacaran|Of Wilpena Group. Includes Wearing Dolomite Member. Overlies Bunyeroo Formation, overlain by Pound Subgroup. Blue - green carbonate rich siltstone and limestone to red - brown siltstone.||||||29-JAN-09
25645|Wonoka Formation|64797|5|Briefly described|p152, p153 Fig.2, p167 Tb.10. |Ediacaran|Ediacaran|See also p169 Fig.12, p176-177. Adelaide Rift Complex. International correlations.|560 Ma.|||||
25645|Wonoka Formation|64829|5|Briefly described|p1084-5 Figs.1,  2|Neoproterozoic|Neoproterozoic|||||||07-FEB-11
25645|Wonoka Formation|64846|5|Briefly described|p211 |Ediacaran|Ediacaran|||||||
25645|Wonoka Formation|65313|6|Mentioned|p576 Fig. 5|Neoproterozoic|Neoproterozoic|||||Overlies Bunyeroo Formation; underlies Pound Subgroup.||26-MAR-12
25645|Wonoka Formation|65410|6|Mentioned|p74.|||Adelaide Geosyncline. Part of Supersequence 3. The upper parts of this unit may be correlated with the Boondawari Formation (Savory Sub-basin).||||||
25645|Wonoka Formation|65892|4|Described|p16, p32-33, p35, p39. |Ediacaran|Ediacaran|Flinders Ranges. Contains large, morphologically complex acritarchs.|c.570 Ma.|Unit in Wilpena Group.|Includes Wearing Dolomite Member.|Overlies Bunyeroo Formation. Is overlain by Bonney Sandstone.|Greenish-grey limestone and siltstone.|
25645|Wonoka Formation|65925|5|Briefly described|Appendix 2.||||||||Shale, grey, calcareous; flaggy dolomite, limestone and silt.|
25645|Wonoka Formation|66569|5|Briefly described|p860, p861 fig.2,|Ediacaran|Ediacaran|Of Wilpena Group. Dolomitic and calcareous marine shelf and turbidite facies. Correlated with Munyarai Formation; underlies Bonney Sandstone; overlies Bunyeroo Formation.||||||
25645|Wonoka Formation|67030|5|Briefly described|p409 Fig. 2, p412 Fig.7, p413 Tab. 2|Ediacaran|Ediacaran|Magnetic information presented for comparison (Schmidt & Williams 2010). Abbreviated as Wonoka Fm in Fig. 2 and Tb. 2||||Overlies the Bunyeroo Formation, underlies the  Bonney Sandstone.||26-APR-12
25645|Wonoka Formation|67484|5|Briefly described|p294 Tb.1, p298-299|Ediacaran|Ediacaran|Adelaide Rift Complex. Contains Palaeopascichnus (Haines, 2000) and Tungussia julia (Grey and Corkeron, 1998) fossils.||Of the Wilpena Group.||Overlain by Bonney Sandstone. Underlain by Bunyeroo Formation. Is correlated with Egan and Julie Formations, and Boonall Dolomite.||
25645|Wonoka Formation|67620|5|Briefly described|p2, 5|Ediacaran|Ediacaran|Adelaide Rift Complex. Post-glacial succession.||Wilpena Group.||Overlies Bunyeroo Formation. Is overlain by Bonney Sandstone (Pound Subgroup). Is correlated with Egan, Julie Formations and Boonall Dolomite.||
25645|Wonoka Formation|67870|5|Briefly described|p9|Ediacaran|Ediacaran|Adelaide Rift System.||Wilpena Group.||||
25645|Wonoka Formation|68030|4|Described|p238-239|Ediacaran|Ediacaran|Flinders Ranges. In the N and S Flinders Ranges, canyons incised 1-1.2 km through the basal Wonoka Formation and underlying formations. Various suggestions by different workers listed on p238.||Unit of Wilpena Group.|Includes Wearing Dolomite Member.|Underlain by Wearing Dolomite Member, and infills incised valleys and canyons cut into the Bunyeroo Formation and ABC Range Quartzite.|Calcareous shale, siltstone and fine sandstone.|
25645|Wonoka Formation|68138|5|Briefly described|p156|Neoproterozoic|Neoproterozoic|Adelaide Rift Complex. Correlations based on common stromatolite (Tungussia sp.) occurrences.||Wilpena Group.||Correlated with Egan Formation and Boonall Dolomite (Kimberley region).||
25645|Wonoka Formation|68269|6|Mentioned|p673-674|||Adelaide Geosyncline.||Wilpena Group||Underlain by Bunyeroo Formation. Overlain by Bonney Sandstone.|Sandstone/siltstone dominated.|
25645|Wonoka Formation|68271|5|Briefly described|p693-696|||Adelaide Rift Complex. ||||Overlain conformably by Billy Springs Formation or Bonney Sandstone. Underlain by Ulupa Siltstone.|Blue-grey calcareous siltstones and light bluish-grey weathering, internally grey limestones.|
25645|Wonoka Formation|68275|6|Mentioned|p56, 60|||||||||
25645|Wonoka Formation|68473|6|Mentioned|p531|||Adelaide Rift Complex.||||||
25645|Wonoka Formation|68713|6|Mentioned|p19||||||Includes the Burr Well Member.|||
25645|Wonoka Formation|69019|3|Fully described|p56-57 Pl.9, p58-60, p144, p164.|||Dalgarno and Johnson (in Thomson et al. 1964); revised by Gostin and Jenkins (1983) to include Wearing Dolomite Member (formerly of Bunyeroo Formation). Type section in Brachina Creek where it is ~500 m thick. Affected by tectonics due to salt withdrawal from underlying strata. Associated with Fe-Mn mineralisation at Village Well Prospect.||Unit in Wilpena Group.|Includes Wearing Dolomite Member and Burr Well Member.|Conformably overlies Bunyeroo Formation.|Basal buff to greenish dolomicrite overlain by cyclic 20-30 mm shale interbeds; locally laminated white dolomicrite; intraformational limestone and hummocky cross-stratified sandstone interbeds.|
25645|Wonoka Formation|70031|5|Briefly described|p245,250-251|Ediacaran|Ediacaran|Adelaide Geosyncline. Ca. 560 Ma date for late Cryogenian to post-Delamerian Orogeny poles. See p250 Table 2 for paleomagnetic analysis.||Unit of Wilpena Group.||Overlain by Bonney Sandstone/Pound Subgroup. Underlain by Bunyeroo Formation.||
25645|Wonoka Formation|70082|6|Mentioned|p2|Ediacaran|Ediacaran|Flinders Ranges.||||||
25645|Wonoka Formation|70333|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic||||||Shale, grey calcareous; flaggy dolomite, limestone and silt.|
25645|Wonoka Formation|70334|4|Described|p2,20,30,36-38,56, 78|Ediacaran|Ediacaran|Geological province: Gawler Craton. Of Stuart Shelf. Prograding calcareous clastic sequence. Deeply incised into the lower parts of the formation, forming major canyons. Wonoka Formation rocks have also been deposited inside incised canyons, with clasts potentially derived from eroded and reworked ABC Range Quartzite and Gawler Range Volcanics rocks. Two main hypotheses for canyon incision: a) canyons cut by fluvial processes following base level change produced by tectonic uplift or Messinian-style sea level change and filled by coastal onlap, or b)  cut in an entirely marine environment (see p37,78 for details).||Unit of Wilpena Group.|||Mixed carbonate-siliciclastic sequence of grey, purple and red calcareous fine-grained siltstone, shale and limestone.|14-OCT-19
25645|Wonoka Formation|70384|5|Briefly described|Map legend.|Ediacaran|Neoproterozoic|Adelaide Geosyncline. Deposits in submarine canyons incised as deep as Ulupa Siltstone. map suggests unit is part of unnamed subgroup.||Of Wilpena Group.|Wearing Dolomite Member, Burr Well Member.||Dark grey, finely laminated, calcareous siltstone; rare grey limestone interbeds in lower sequence. Where no obvious erosive base, comprises highly condensed cyclic shale grading to dolomicrite. Intraformational limestone and sandstone interbeds.|23-JAN-19
25645|Wonoka Formation|70406|6|Mentioned|p125, 127, 121, Fig 5|||||Of Depot Springs Group||||
25645|Wonoka Formation|70407|4|Described|p110-111, p108, p109, 105|Neoproterozoic|Neoproterozoic|Age: Ediacaran. Divided in to 11 informal lithofacies units.||Of Depot Springs Subgroup.||Overlies Wearing Dolomite. Gradationally overlain by Bonney Sandstone near Mount Goddard.|greyish red fine-grained sandstone and interbedded calcareous shale; greenish limestones; mixed carbonate/ siliciclastic succession.|
25645|Wonoka Formation|70416|6|Mentioned|p75|||In Bunyeroo Gorge, Adelaide Rift Complex, this unit contained the stromatolite Tungussia julia. Now the basal Bonney Sandstone.||||||
25645|Wonoka Formation|70790|5|Briefly described|p258 Fig.1, p259|Ediacaran|Ediacaran|Adelaide Rift Complex.|||||Mainly clastic mudstones.|
25645|Wonoka Formation|71129|5|Briefly described|p128|Ediacaran|Ediacaran|Of Adelaide Geosyncline.||Unit of Wilpena Group.||||
25645|Wonoka Formation|71237|14|Not recorded|p10, 19|||||||||
25645|Wonoka Formation|71241|2|Defined|p13, 14, 19, p9-10|||||Of Wilpena Group.||Gradational contact with underlying Bunyeroo Formation in type section.||
25645|Wonoka Formation|71242|14|Not recorded|p10, 11|||||||||
25645|Wonoka Formation|71250|5|Briefly described|p70|Ediacaran|Ediacaran|Central Flinders Ranges.||Wilpena Group.|Wearing Dolomite Member.|Overlies Bunyeroo Formation. Is overlain by Bonney Sandstone (Pound Subgroup).||
25645|Wonoka Formation|71288|6|Mentioned|p146|||Implications of a c.570 Ma paleopole position from this unit discussed.||||||
25645|Wonoka Formation|72449|5|Briefly described|p1, p2 Map Legend|Neoproterozoic|Neoproterozoic|Includes grazing trails of small worms. First good evidence of marine animal life.||||Overlies Bunyeroo Formation and underlies Bonney Sandstone.|Green-grey laminated siltstone and thin limestone. Sandstone and grey blue stromatolitic limestone at top.|
25645|Wonoka Formation|72451|4|Described|p4 fig 1, p5|Late Proterozoic|Late Proterozoic|Appears concordant [conformable] over Bunyeroo Formation in places but fills submarine canyons through much [more] of the Wilpena Group in other places. Depositional environment: lagoonal to near shore storm base. Contains load casts, lenticular bedding, slump folds and ooid grainstone horizons.||||Overlies Bunyeroo Formation, unconformably.|Grey to white silty and fine sandy limestone that is well laminated and often crossbedded.|09-JUN-20
25645|Wonoka Formation|72456|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Marree 1:250k map sheet. |||||Shale, grey, calcareous; flaggy dolomite, limestone and silt.|
25645|Wonoka Formation|72489|4|Described|p2, p3, p4, p5 Fig.4, p5-6, p7 Fig.6|Ediacaran|Ediacaran|Adelaide Rift Complex. See also p8 Fig.7, p8-9, p11, p14. Includes cross-stratified, laminated and hummocky limestone. Described as mid-Ediacaran age.||||Overlies Bunyeroo Formation. Underlies Elatina Formation, [Goyder Formation - ?this unit in Amadeus Basin] and Bonney Sandstone.|Includes limestones and siliciclastic sediments.|
25645|Wonoka Formation|73093|5|Briefly described|map legend|Neoproterozoic|Neoproterozoic||||||Mixed carbonate-siliciclastic sequence. Mudstone, calcareous and dolomitic sandstone, limestone, siltstone.|09-DEC-21
25645|Wonoka Formation|73110|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic||||||Shale, grey, calcareous; flaggy dolomite, limestone and silt.|
25645|Wonoka Formation|73188|6|Mentioned|p315, p352|||Flinders Ranges.||||||
25645|Wonoka Formation|73222|4|Described|p6-8, p11-12, p14, p16-21, p23-26|Ediacaran|Ediacaran|Adelaide Rift Complex. Includes informal lower, middle and upper limestone members and a green siltstone member (lithofacies 1-4 respectively) [Described in moderate detail building on previous work but formal names are not given; see article for more detail]. Interpreted herein as deposited in a lagoon/lacustrine environment. Forms inclusions in the Patawrta Diapir (and in adjacent suprasalt and subsalt minibasins), which suggests active halokinesis during the Ediacaran. Documents the Shuram [negative carbon isotope] excursion in strata adjacent to Patawarta Diapir but inclusions within the diapir are diagenetically altered. [Article includes O and C stable isotope investigation].||Wilpena Group, Heysen Supergroup|[see comments]|||
25645|Wonoka Formation|73236|6|Mentioned|p40|||Flinders Ranges.||Wilpena Group, Heysen Supergroup||||
25645|Wonoka Formation|73255|6|Mentioned|p532, p534|Ediacaran|Ediacaran|Contains Palaeopascichnus and Tungussia julia fossils.||||Overlies the Bunyeroo Formation, underlies the Bonney Sandstone.||
25645|Wonoka Formation|74367|6|Mentioned|p7 Fig.6, p19|||||Wilpena Group||||
81435|Woodendinna Dolostone|70833|5|Briefly described|p176,180,184,187-188,190,200-201,203|Terreneuvian|Terreneuvian|Of Arrowie Basin. Key sections: MORO (S of Moro Gorge, Arrowie Syncline); WILK (Bunkers Graben); 10MS-W (Ten Mile South, SE Bunkers Graben).  Highstand systems tract. Depostional environment: shallow marine carbonate shelf to supratidal settings.||Unit of Hawker Group.||Overlain (locally disconformably) by Mount Mantell Member/Wilkawillina Limestone. Conformably underlain by Parachilna Formation.|Microbialites, oncolites and low stromatolite bioherms.|21-AUG-19
81435|Woodendinna Dolostone|70835|6|Mentioned|p336-337|Cambrian|Cambrian|Arrowie Basin, Flinders Ranges.||||Overlies Parachilna Formation. Is overlain by Wirrapowie or Wilkawillina Limestones.||
81435|Woodendinna Dolostone|71102|5|Briefly described|p252,267|Terreneuvian|Terreneuvian|Of Arrowie Basin.||||Overlain by Wirrapowie and Wilkawillina limestones. Underlain by Parachilan Formation.||
27954|Woodgate Gravel|40910|6|Mentioned|p20|||||||||
27954|Woodgate Gravel|40911|6|Mentioned|Map legend|late Pleistocene|late Pleistocene|||||||
27954|Woodgate Gravel|40925|6|Mentioned|Map legend|Cenozoic|Cenozoic|||||||19-NOV-08
27954|Woodgate Gravel|40926|3|Fully described|p30|||||||||
76224|Wookata Shale Member|72429|3|Fully described|p952, p956, p965, p967, p970-971, p974|Lower Cambrian|Lower Cambrian|Mount Chambers Gorge, eastern Flinders Ranges. Up to 23m thick in measured section. Provides a useful marker bed to separate and trace the massive limestones of the Moorowie Formation in the field. Exposure of units is well exposed as concave ground between limestone beds. Contains thin interbeds (20-50mm thick) of light grey limestone. Interbeds commonly include small intraclasts of siltstone, sand, dolostone, quartz, feldspar and thin sideritic lenses. Linguoid sole and ripple markings are common and suggest tidal currents reworked smi-lithified siltstone on the tidal flats. Mud cracks record periodic exposure of a tidal terrace, while tidal pools host sparse fossil fauna, including trilobites. Considered here to be a shallow, lightly channelised, shallow marine littoral ramp facies, seaward of the platform margin with some adjacent tidal flats.||Moorowie Formation||Overlies the Pinyatta Member. Underlies the Kandramooka Member. Probable equivalent of and grades into the Oraparinna Shale.|Purple, ferric red-brown to khaki green finely micaceous shales with thin limestone interbeds at base. Ripple marks, rare trilobite tracks.|
31510|Woolpunda Marl Member|23226|2|Defined|p897|Miocene|Longfordian|Age: late Longfordian to early Miocene. Laterally equivalent to Cowirra Clay and Portee Carbonate Members. Lithology and macrofauna are very similar to the Murbko Marl Member and Winnambool Fm. but distinguishable by age and strat position. Of Finniss Fm.||||||
31510|Woolpunda Marl Member|64237|5|Briefly described|p19 Fig. 2b|Middle Miocene|Early Miocene|Of the Finniss Formation (Murray Group). Originally introduced as a new member with the stratigraphic revision of the Murray Group up to Murray Supergroup by Lukasic and James (1998), but retained when Murray Group was reinstated.||||||
27940|Woolshed Flat Shale|22869|5|Briefly described|P38, P45, Fig3||Neoproterozoic|Underlying unit is Basket Range Sandstone||||||
27940|Woolshed Flat Shale|22889|5|Briefly described|p34-35|Adelaidean|Adelaidean|Parent - Bungarider Subgroup.  Formerly part of the Mundallio Subgroup but has been redefined to be encorporated into the Bungarider Subgroup, see p30 for details of change.||||||
27940|Woolshed Flat Shale|23482|5|Briefly described|p10|Adelaidean|Adelaidean|||||||
27940|Woolshed Flat Shale|23731|6|Mentioned|p29|Adelaidean|Adelaidean|||||||
27940|Woolshed Flat Shale|24175|6|Mentioned|p11|Neoproterozoic|Neoproterozoic|||||||
27940|Woolshed Flat Shale|24176|5|Briefly described|p11, p25 Tb. 1|Adelaidean|Adelaidean|Age is Torrensian. Equivalent to Myrtle Springs Formation of the Burra Group. Geological Province: Mount Painter Province.||||||27-MAY-08
27940|Woolshed Flat Shale|29780|6|Mentioned|p26|||||||||
27940|Woolshed Flat Shale|30176|6|Mentioned|Map legend|Adelaidean|Adelaidean|EquivalentTorrensian||||||
27940|Woolshed Flat Shale|30177|6|Mentioned|p66|||||||||
27940|Woolshed Flat Shale|30801|6|Mentioned|p5|||Torrensian. Table P5-6||||||07-NOV-22
27940|Woolshed Flat Shale|31292|6|Mentioned|p6|||Refers Wilson (1952)||||||
27940|Woolshed Flat Shale|32508|6|Mentioned|p119|||||||||
27940|Woolshed Flat Shale|32547|6|Mentioned|Fig.2|||Torrensian||||||
27940|Woolshed Flat Shale|32724|6|Mentioned|Fig.1|||Correlation. Torrensian||||||
27940|Woolshed Flat Shale|33033|6|Mentioned|p68|||See also p69||||||07-NOV-22
27940|Woolshed Flat Shale|33034|6|Mentioned|p63|||||||||
27940|Woolshed Flat Shale|33422|6|Mentioned|Map legend|Precambrian|Precambrian|||||||
27940|Woolshed Flat Shale|33423|4|Described|p12|||Equiv. described.||||||
27940|Woolshed Flat Shale|33659|4|Described|p7|||Regional geology,hydrology etc.||||||
27940|Woolshed Flat Shale|33951|6|Mentioned|p7|||Soil development||||||
27940|Woolshed Flat Shale|33956|4|Described|p1040|||||||||
27940|Woolshed Flat Shale|34320|6|Mentioned|Fig.|||Regional geology plan.||||||
27940|Woolshed Flat Shale|34536|6|Mentioned|Map legend|Adelaidean|Adelaidean|Torrensian||||||
27940|Woolshed Flat Shale|34587|5|Briefly described|p36|||||||||
27940|Woolshed Flat Shale|34957|6|Mentioned|p396|||||||||
27940|Woolshed Flat Shale|34979|6|Mentioned|p33|||||||||
27940|Woolshed Flat Shale|35090|6|Mentioned|Fig.1|||||||||
27940|Woolshed Flat Shale|35357|6|Mentioned|p21|||||||||
27940|Woolshed Flat Shale|36834|6|Mentioned|p25|||||||||
27940|Woolshed Flat Shale|36835|6|Mentioned|p31|||||||||
27940|Woolshed Flat Shale|37461|6|Mentioned|Table 5.I|||||||||
27940|Woolshed Flat Shale|38157|6|Mentioned|Table III|||||||||
27940|Woolshed Flat Shale|38926|4|Described|p29|||||||||
27940|Woolshed Flat Shale|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Torrensian||||||
27940|Woolshed Flat Shale|39350|6|Mentioned|Map legend|Adelaidean|Adelaidean|Torrensian||||||
27940|Woolshed Flat Shale|39351|6|Mentioned|Map legend|Adelaidean|Adelaidean|Torrensian||||||
27940|Woolshed Flat Shale|40294|6|Mentioned|p32|||||||||
27940|Woolshed Flat Shale|40442|5|Briefly described|p8|||See also Fig.4.||||||
27940|Woolshed Flat Shale|40456|6|Mentioned|Fig.2|||||||||
27940|Woolshed Flat Shale|40500|6|Mentioned|p142|||||||||
27940|Woolshed Flat Shale|40501|6|Mentioned|p115|||||||||
27940|Woolshed Flat Shale|40852|6|Mentioned|Fig.3.2|||||||||
27940|Woolshed Flat Shale|41404|4|Described|p105|||||||||
27940|Woolshed Flat Shale|41494|6|Mentioned|p30|||||||||
27940|Woolshed Flat Shale|41526|6|Mentioned|p45|||||||||
27940|Woolshed Flat Shale|42093|6|Mentioned|p6|||||||||
27940|Woolshed Flat Shale|42098|6|Mentioned|p51|||||||||
27940|Woolshed Flat Shale|42222|5|Briefly described|p13|||||||||
27940|Woolshed Flat Shale|42236|6|Mentioned|Fig.2 P106|||||||||
27940|Woolshed Flat Shale|42238|5|Briefly described|p72|||||||||
27940|Woolshed Flat Shale|42505|5|Briefly described|Map legend|Adelaidean (Torrensian)|Adelaidean (Torrensian)|||||||
27940|Woolshed Flat Shale|42506|5|Briefly described|Map legend|Adelaidean (Torrensian)||||||||
27940|Woolshed Flat Shale|42733|6|Mentioned|map legend|Adelaidean||||||||
27940|Woolshed Flat Shale|43052|5|Briefly described|p179,Table 6.1|||Of Mundallio Subgroup.||||||27-MAY-08
27940|Woolshed Flat Shale|44133|6|Mentioned|p46|||||||||
27940|Woolshed Flat Shale|44690|4|Described|map legend|||Geol. Atlas Series. (I/54-5). Torrensian.||||||
27940|Woolshed Flat Shale|50615|6|Mentioned|p304, Fig. 3|||Name used interchangeably with Woolshed Flat Formation. Geological Province: Adelaide Fold Belt.||||||
27940|Woolshed Flat Shale|61307|5|Briefly described|p25 Fig. 14|Torrensian|Torrensian|Of the Burra Group. Geological Province: Adelaide Fold Belt.||||||
27940|Woolshed Flat Shale|62724|5|Briefly described|p17 Fig. 4|Torrensian|Torrensian|Of the Bungarider Subgroup (Burra Group).||||||07-FEB-11
27940|Woolshed Flat Shale|64647|6|Mentioned|p40|||Laminated metasiltstone.||||||
27940|Woolshed Flat Shale|65379|5|Briefly described|p643, p644|Neoproterozoic|Neoproterozoic|Of Burra Group (Warrina Supergroup). Shale, black; dolomitic siltstone; dolomite; grey laminated siltstone. N.B.  Asbestos deposit host, contains Smiths and Berry asbestos mines.||||||07-MAR-12
27940|Woolshed Flat Shale|66194|6|Mentioned|p588|||Precambrian.||||||09-MAR-12
27940|Woolshed Flat Shale|66522|5|Briefly described|p23.|Neoproterozoic|Neoproterozoic|||Unit in Bungarider Subgroup. |||Laminated siltstone with variable carbonate content and lenticular thin sandy interbeds.|
27940|Woolshed Flat Shale|69019|6|Mentioned|p39.|Neoproterozoic|Neoproterozoic|||||||
27940|Woolshed Flat Shale|70405|6|Mentioned|p51 table 4|Neoproterozoic|Neoproterozoic|||Bungarider Subgroup||||
27940|Woolshed Flat Shale|70819|5|Briefly described|p11, 13, 18|Neoproterozoic|Neoproterozoic|Clare Valley.||Bungarider Subgroup.||Overlies Skillogalee Dolomite. Is overlain by Watervale Sandstone.|Deeper shelf silty sediments.|
27940|Woolshed Flat Shale|71240|2|Defined|p6,p9, p19|||||||||
27940|Woolshed Flat Shale|72450|5|Briefly described|Brochure map|||||Burra Group|||Laminated and sandy grey-green siltstone.|
27940|Woolshed Flat Shale|73188|5|Briefly described|p316, p323-328, p332, p336, p339|Neoproterozoic|Neoproterozoic|Mount Lofty Ranges.||Bungarider Subgroup, Burra Group||Overlain by Stonyfell Quartzite.|Siltstone, carbonaceous shale and phyllite.|
27940|Woolshed Flat Shale|74367|6|Mentioned|p7 Fig.6|||||Bungarider Subgroup||||
79318|Wortham Granite|71037|5|Briefly described|p22-23 Fig.2|Paleoproterozoic|Paleoproterozoic|Shown only on the Six Mile Hill 1:75,000 surface geology map (p22-23 Fig.2). U-Pb SHRIMP age 1747+/-13 Ma.|c. 1747 +/- 13 Ma.|Of Moola Suite.||Shown as younger than Wandearah Formation.|Granite, medium-grained, equigranular, pink, K-feldspar, quartz, minor plagioclase, biotite, trace tourmaline, opaques, zircon, weakly foliated.|
79318|Wortham Granite|71129|4|Described|p21,40-41,44,74,177,205,225,227|Statherian|Statherian|Geological Province: Spencer Domain, Gawler Craton. Exposed as low outcrops and subcrops extending over an area !500 m x 400 m wide, ~3 km SW of Wortham Dam to the west of the Roopena Fault Zone ~1.5 km to the south of SIX MILE HILL. Intruded into Broadview Schist as a pluton immediately prior to, or during early stages of 1740-1690 Ma Kimban Orogeny. Metaluminous and ferroan, alkali-calcic in composition with high silica content. HREE-enriched with distinct Eu anomaly; interpreted to be derived from crustal melting of the Sleaford Complex and/or Cooyerdoo Granite. Magmatic crystallisation age of 1747+\-3 Ma (Jagodzinski and McAvaney 2016).|1747+\-3 Ma (magmatic; SHRIMP U-Pb)|Unit of Moola Suite.||Intruded into Broadview Schist.|Pink medium-grained equigranular granite composed of K-feldspar, quartz, plagioclase, biotite and trace tourmaline, opaques and zircon.|
79318|Wortham Granite|71130|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Geochronology by Jagodzinski and McAvaney (2016).|1747 +/- 13 Ma (SHRIMP U-Pb).||||Granite, medium-grained, equigranular, pink, K-feldspar, quartz, minor plagioclase, biotite, trace tourmaline, opaques, zircon. Weakly foliated.|
79318|Wortham Granite|71131|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Geochronology by Jagodzinski and McAvaney (2016).|1747 +/- 13 Ma (SHRIMP U-Pb).|Moola Suite.|||Granite, medium-grained, equigranular, pink, K-feldspar, quartz, minor plagioclase, biotite, trace tourmaline, opaques, zircon. Weakly foliated.|
79318|Wortham Granite|71862|2|Defined|p6-p9, p22, p25|Statherian|Statherian|Named for Wortham Dam, Roopena Station, ~30 km northwest of Whyalla, Eyre Peninsula where it is exposed as low outcrops and subcrops. In the subsurface this unit is defined as magnetic high trending north-northwest and is 750m wide with a linear extent of 8km. The type locality is defined as low outcrops located ~10km south-southwest of Roopena Homestead, Roopena Station comprising the area extending 100m radially from the point 719075mE, 6368945mN, GDA94, Zone 53. Age is a SHRIMP U-Pb date interpreted as the age of magmatic crystallisation. Geochemistry is discussed. See also p28-p29, p41, p53, p55.|1747 +/- 13 Ma (Jagodzinski & McAveny, 2017)|Moola Suite||Intrudes (inferred) the Broadview Schist.|Weakly-foliated, orange-pink, medium-grained, equigranular granite composed of K-feldspar and quartz with minor plagioclase and biotite and trace tourmaline, opaques and zircon.|20-APR-23
79318|Wortham Granite|73110|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|||Moola Suite.|||Granite, medium-grained, equigranular; pink, K-feldspar, quartz, minor plagioclase, biotite, trace tourmaline, opaques, zircon; weakly foliated.|
79318|Wortham Granite|73525|5|Briefly described|p19 Fig.13|Statherian|Statherian|Spencer Domain.|1747+/-13 Ma crystallisation age|Moola Suite|||Felsic intrusive.|
27258|Wortupa Quartzite|22869|6|Mentioned|P46|||Correlated to the Carey Gully Sandstone Member||||||
27258|Wortupa Quartzite|22889|6|Mentioned|p31|Adelaidean|Adelaidean|Parent - Emeroo Subgroup.||||||
27258|Wortupa Quartzite|23394|5|Briefly described|Map legend|Proterozoic|Proterozoic|||||||
27258|Wortupa Quartzite|23411|6|Mentioned|Map Legend|||||||||
27258|Wortupa Quartzite|23818|5|Briefly described|p55|||Underlying unit: Opaminda Siltstone. Of the Burra Group. Equivalent to the Rhynie Sandstone.||||||
27258|Wortupa Quartzite|24176|4|Described|p10, p25 Tb. 1|Adelaidean|Adelaidean|Of Burra Group.  Quartzite, arkosic grit, conglomerates.  Age is Torrensian.  Max. thickness: 305m.  Overlain by Skillogalee Dolomite.  Geological Province: Mount Painter Province.||||||
27258|Wortupa Quartzite|24546|5|Briefly described|p2 - 3 Fig.2|Neoproterozoic|Neoproterozoic|Of Burra Group. Overlies River Wakefield Subgroup. Geological Province: Adelaide Fold Belt.||||||16-JAN-08
27258|Wortupa Quartzite|24593|5|Briefly described|p613 Fig. 1b|||Of the Burra Group.  Geological Province: Mount Painter Inlier.||||||
27258|Wortupa Quartzite|30176|6|Mentioned|Map legend|Adelaidean|Adelaidean|Torrensian||||||
27258|Wortupa Quartzite|30177|2|Defined|p128|Adelaidean|Adelaidean|See also p64. Type section: South of Arkaroola track, 1.6 miles northwest of Arkaroola Homestead, lat. 30degrees 19'08"S long. 139degrees20'57"E to lat. 30degrees 19'12 S long. 139degrees20'54"E.||||||25-NOV-22
27258|Wortupa Quartzite|30801|6|Mentioned|p5|||Torrensian. Table P5-6.||||||
27258|Wortupa Quartzite|30807|6|Mentioned|p103|||Suggested map symbol||||||
27258|Wortupa Quartzite|32724|6|Mentioned|Fig.1|||Torrensian. Correlation||||||
27258|Wortupa Quartzite|33474|6|Mentioned|Fig.4|||||||||
27258|Wortupa Quartzite|33693|6|Mentioned|p153|||||||||
27258|Wortupa Quartzite|34535|5|Briefly described|p55|||Equiv. Rhynie Sst. P59||||||
27258|Wortupa Quartzite|35255|6|Mentioned|p41|||||||||
27258|Wortupa Quartzite|35328|6|Mentioned|p11|||||||||
27258|Wortupa Quartzite|36733|6|Mentioned|Table 5|||||||||
27258|Wortupa Quartzite|37461|6|Mentioned|Table 5.I|||||||||
27258|Wortupa Quartzite|37854|6|Mentioned|p15|||See also Table 1.||||||
27258|Wortupa Quartzite|38157|6|Mentioned|Table III|||||||||
27258|Wortupa Quartzite|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Torrensian||||||
27258|Wortupa Quartzite|40294|6|Mentioned|p8|||See also Table 1||||||
27258|Wortupa Quartzite|41404|3|Fully described|p86|||||||||
27258|Wortupa Quartzite|41405|6|Mentioned|Fig.55|||||||||
27258|Wortupa Quartzite|42222|6|Mentioned|Table 1 P5|||||||||
27258|Wortupa Quartzite|43052|5|Briefly described|p177,Table 6.1|||of Emeroo Subgroup||||||
27258|Wortupa Quartzite|61523|5|Briefly described|p12|Adelaidean|Adelaidean|Geological Province: Mount Painter Province.||||||
27258|Wortupa Quartzite|65925|5|Briefly described|p124 Fig.3, p125, Appendix 2.|||||Unit in Burra Group.||Overlies Opaminda Formation.|Sandstone, grey-green, well bedded; quartzite, pale grey; minor dark grey siltstone; arkosic grit; conglomerate.|
27258|Wortupa Quartzite|70384|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Adelaide Geosyncline.||Emeroo Subgroup.||Conformably? overlies Opaminda Formation.|Grey-green, well-bedded sandstone; pale grey quartzite; minor dark grey siltstone; arkosic grit; conglomerate.|
82036|Worumba Dolomite|72492|5|Briefly described|p2 Fig.1, p3-4, p4 Fig.3e, p5, p6|Neoproterozoic|Neoproterozoic|Includes the Worumba Shale Member? Written as Worumba Dolomite Beds on p2. See also p5 Fig.5a and b, p6, p11 Tb.2 and 3, p11 Fig.7, p13-14 Tb.4, p16.||Curdimurka Subgroup||Overlies Waraco Limestone.|Includes crossbeds and halite casts and wavy laminated and often stromatolitic dolomite with stromatolitic carbonate with nodular gypsum or anhydrite pseudomorphs.|
82036|Worumba Dolomite|73222|6|Mentioned|p7|Tonian|Tonian|Flinders Ranges. Torrensian.||Curdimurka Subgroup, Callanna Group, Warrina Supergroup||Underlain by Waraco Limestone.||
74643|Wynbring Granite|40644|6|Mentioned|p132, p133 Fig. 17|Paleoproterozoic|Paleoproterozoic|Name is probably not intended to be formal. Age: ca. 1701+/-30Ma. granitic gneiss rocks.||||||07-NOV-08
74643|Wynbring Granite|64137|6|Mentioned|p1553 Fig.8 |||Neodymium isotope data.||||||
74643|Wynbring Granite|65390|6|Mentioned|p22 Fig. 3|Statherian|Statherian|Christie Domain, Gawler Craton. Age of 1685 Ma given.||||||
75850|Yabmana Iron Formation|66882|5|Briefly described|p103 Fig.3c|Orosirian|Orosirian|Lincoln-Cleve uplands.||Darke Peak Group||Overlies Poolalalie Dolomite, underlies Bosanquet Formation.||05-MAR-15
75850|Yabmana Iron Formation|73525|5|Briefly described|p19 Fig.13|||Cleve Domain.||Darke Peak Group||||
24130|Yadnarie Schist|22629|6|Mentioned|p149,150|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
24130|Yadnarie Schist|23285|5|Briefly described|Fig 3 p 333|||||||||
24130|Yadnarie Schist|23719|4|Described|p14|Paleoproterozoic|Paleoproterozoic|See also page 14 table 1. Of Hutchinson Group. O'lying unit Myola Volcanics. U'lying unit Middleback Subgroup. Geol. Province: Gawler Craton. Max. thickness: >1000 m.||||||07-NOV-08
24130|Yadnarie Schist|37811|2|Defined|p238|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
24130|Yadnarie Schist|38969|6|Mentioned|p220|||||||||
24130|Yadnarie Schist|39345|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
24130|Yadnarie Schist|39349|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
24130|Yadnarie Schist|39353|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
24130|Yadnarie Schist|40448|4|Described|p30|||||||||
24130|Yadnarie Schist|41667|5|Briefly described|p55|||Also Mention P5||||||
24130|Yadnarie Schist|42738|5|Briefly described|map legend|Paleoproterozoic||||||||07-NOV-08
24130|Yadnarie Schist|43052|5|Briefly described|p61|||Of Middleback Subgroup.||||||27-MAY-08
24130|Yadnarie Schist|50605|5|Briefly described|p3.3, 5.4|||Of the Hutchison Group. Geological Province: Gawler Craton & Curnamona Province.||||||
24130|Yadnarie Schist|61307|5|Briefly described|p37|||Of the Hutchison Group (upper part). Pelitic to semi-pelitic schists. Geological Province: Gawler Craton. ||||||
24130|Yadnarie Schist|62893|4|Described|Map Legend, p10-11, p13, p28, p36|Early Proterozoic|Early Proterozoic|Only recognised in the Cleve Uplands. Represents a major period of regression. Minimum thickness of 1000 m; upper contact not exposed. The type section is just north of Mangalo Creek. Similar in outcrop appearance to the Cook Gap Schist, but with a greater proportion of muscovite and amphibolite is absent. In the Cockabidnie area are iron-stained, quartz-sericite banded metasiltstone with sericite porphyroblasts after sillimanite, and minor interlayered quartz-magnetite gneiss.||Hutchison Group|||Quartz-veined, fine grained, quartz-feldspar-biotite-muscovite schist interlayered with psammitic bands up to several centimetres thick.|
24130|Yadnarie Schist|65376|5|Briefly described|p54. |Paleoproterozoic|Paleoproterozoic|||Unit in Hutchison Group.|||Pelitic schist.|
24130|Yadnarie Schist|65390|5|Briefly described|p17|Paleoproterozoic|Paleoproterozoic|Upper, pelitic, sequence of Hutchison Group.||||||
24130|Yadnarie Schist|65922|5|Briefly described|p15|Orosirian|Orosirian|Gawler Craton. Of Middleback Subgroup, Hutchison Group. Overlies Upper Middleback Jaspilite. Compositionally similar to Cook Gap Schist. Does not outcrop in this map area.||||||
24130|Yadnarie Schist|66302|6|Mentioned|p24|||||Hutchison Group||||
24130|Yadnarie Schist|66882|5|Briefly described|p101, p103 Fig.3a,c, p106-107, p109-114|Statherian|Statherian|Lincoln-Cleve uplands. Formerly in upper part of Hutchison Group. Isotope data. Geochemistry discussed.|1784+/-18 Ma.|Cleve Group.||Overlies Mount Shannon Iron Formation.|Succession of pelitic schist.|05-MAR-15
24130|Yadnarie Schist|67323|6|Mentioned|Eastern Australia Time-Space Plot|||Southern Gawler Craton.||||||
24130|Yadnarie Schist|68131|5|Briefly described|p57-58|||Eastern Eyre Peninsula. Appears as Yardnarie Schist on p58.||Hutchison Group.|||Pelitic schist.|
24130|Yadnarie Schist|73103|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic||||||Schist, quartz-feldspar-biotite-muscovite. Locally quartz-sericite banded metasiltstone, sericite porphyroblasts after sillimanite; minor interlayered quartz-magnetite gneiss.|
34345|Yaltipena Formation|22510|5|Briefly described|table1p37,41|||Of the Upalinna Subgroup.  Age: marinoan. Central Flinders Ranges||||||13-OCT-04
34345|Yaltipena Formation|22911|5|Briefly described|38|||Underlying unit Trezona Formation||||||
34345|Yaltipena Formation|23250|5|Briefly described|p1122, p1124 Fig.2||Cryogenian|Of Umberatana Group. Formerly Yaltipena Member. Correlate Wilmington Formation equivalent and Olympic Formation.||||||
34345|Yaltipena Formation|60959|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Of the Upalinna Subgroup. Limestone with sandy beds, calcareous siltstone.||||||
34345|Yaltipena Formation|61236|6|Mentioned|p24 Fig. 1|Adelaidean|Adelaidean|||||||
34345|Yaltipena Formation|61732|5|Briefly described|p28 Fig. 13|Marinoan|Marinoan|Of the Upalinna Subgroup (Umberatana Group). Geological Province: Adelaide Rift Complex.||||||07-FEB-11
34345|Yaltipena Formation|62085|6|Mentioned|p18, p20 fig 5, p21 fig 6|Cryogenian|Cryogenian|Pre-glacial.||||Overlies Trezona Formation. Is overlain unconformably by Elatina Formation.|Siltstone.|
34345|Yaltipena Formation|62592|5|Briefly described|p50 Table 5.1.|Marinoan|Marinoan|Adelaide Geosyncline.||Unit in Upalinna Subgroup.||Overlies Trezona Formation.|Siltstone.|
34345|Yaltipena Formation|64801|6|Mentioned|p110 Fig.2, p112|Neoproterozoic|Neoproterozoic|Adelaide Rift Complex.||Umberatana Group.||||
34345|Yaltipena Formation|65892|5|Briefly described|p33 Fig.18, p37 Fig.20. |Cryogenian|Cryogenian|||Unit in Umberatana Group.||Overlies Trezona Formation. Is overlain by Elatina Formation.||
34345|Yaltipena Formation|66464|4|Described|p167, p170, p173, p177|Cryogenian|Cryogenian|Adelaide Rift Complex. Overlies and may be partly contemporaneous with Trezona Formation. Contains fine terrigenous sandstones and siltstones with mudcrack and rain imprints, indicating intermittent subaerial exposure. Overlain by Elatina Formation.||||||
34345|Yaltipena Formation|67030|6|Mentioned|p412 Fig. 7, p413 Tb. 2|Cryogenian|Cryogenian|Magnetic information presented for comparison (Sohl et al. 2009). Abbreviated as Yaltipena Fm in p413 Tab. 2||||||26-APR-12
34345|Yaltipena Formation|70031|4|Described|p245,248,250-251|Cryogenian|Cryogenian|Adelaide Geosyncline. Upper interglacial succession. Thickness: 111 m. Transgressive-regressive clastic unit and marks the end of overall lowering of sea level and the start of the Elatina glaciation (Mawson 1949; Williams et al., 2008, 2011). Boulders at the base of the Elatina Formation were bulldozed into the Yaltipena Formation by ice action, indicating that the topmost beds of the Yaltipena were then unlithified (Lemon and Reid 1998; Williams et al., 2008). See p250 Table 2 for paleomagnetic analysis.||Unit of Trezona Formation.||Overlain unconformably by Elatina Formation/Yerelina Subgroup. Underlain unconformably by Trezona Formation.|Red bed clastics.|
34345|Yaltipena Formation|71288|6|Mentioned|p136, 139-140|Neoproterozoic|Neoproterozoic||650-635 Ma.|||||
34345|Yaltipena Formation|72473|6|Mentioned|p4|||||||||
34345|Yaltipena Formation|72613|6|Mentioned|p11, p15|Cryogenian|Cryogenian||||||Marine red beds.|
34345|Yaltipena Formation|73234|6|Mentioned|p20|||||||||
34345|Yaltipena Formation|74367|5|Briefly described|p7 Fig.6, p8-9, p11, p16-17, p20, p22|Cryogenian|Cryogenian|See also p14.|662+/-20 Ma LA-ICP-MS detrital zircon MDA|Upalinna Subgroup||||
24136|Yandruwantha Sand|13497|5|Briefly described|p115, p115 fig 6.33|Quaternary|Pliocene|Lake Eyre Basin. Consists of aeolian dune, fluvial, saline lake, gibber plains and palaeosol deposits. ||||Unconformably overlies the Namba Formation. Overlain by the Millyera Formation.||
24136|Yandruwantha Sand|23154|5|Briefly described|Map Legend|Pleistocene|Pleistocene|Geological Province - Lake Eyre Basin - Callabonna Basin.||||||
24136|Yandruwantha Sand|23155|4|Described|p36|Cenozoic|Cenozoic|Location of type section advised p36.  The unit is only known from drillhole cuttings and is probably partly Kutjitara Formation equivalent and may include equivalents of the Katipiri Sand and Tirari Formation of the Tirari Desert area.||||||19-NOV-08
24136|Yandruwantha Sand|23478|5|Briefly described|p28|Pleistocene|Miocene|||||||
24136|Yandruwantha Sand|42543|3|Fully described|p2-7|||Name reserved, but 'geographic' part of name invalid as described herein.||||||
24136|Yandruwantha Sand|44133|5|Briefly described|p245|Pleistocene|Pleistocene|Correlative of the Kutjitara Formation.||||||
24136|Yandruwantha Sand|68068|5|Briefly described|Map legend|Miocene|Miocene|Callabonna Sub-basin, Lake Eyre Basin.|||||Medium to very coarse, loose brown sand with rough, subangular grains; varying proportion of white clayey fine sandstone grains and yellow to red coated grains; contains reworked Mesozoic and Tertiary sand with aeolian input.|
24136|Yandruwantha Sand|69023|4|Described|p109, p112, p117, p124-125, p140-141|Cenozoic|Cenozoic|Of Callen (1992). Type section in Kirralee 1 well on STRZELECKI map. Its pale colour distinguishes this unit from the darker Eyre Formation. Known only from well cuttings; usually covered by younger alluvium. Is probably partly equivalent to Kutjitara Formation, Katipiri Sand and Tirari Formation. Sediment probably sourced from Eyre and Namba Formations.||||Overlies Namba Formation unconformably. May interdigitate with overlying Willawortina Formation.|A mixture of alternating white or orange beds of fine to gravelly quartz sand with rather irregular angular grains; commonly poorly sorted. Presence of pebbly lenses, white sand, and a well-washed appearance are characteristic. Massive gypsum cap.|
24136|Yandruwantha Sand|69947|5|Briefly described|p13 Fig.7.2|Pliocene|Pliocene|Callabonna Sub-basin, Lake Eyre Basin.||||||
24136|Yandruwantha Sand|71342|6|Mentioned|Ch7 p13|Late Pliocene|Late Pliocene|||||Unconformably overlies the Namba Formation. Overlain by the Millyera Formation.||
79744|Yannabie Rhyolite Member|70659|5|Briefly described|p8|Mesoproterozoic|Mesoproterozoic|Gawler Ranges.||Eucarro Rhyolite.||||
79744|Yannabie Rhyolite Member|70816|5|Briefly described|p5|||Gawler Ranges region.||Unit of Eucarro Rhyolite||Overlain by, and laterally equivalent to Paney Rhyolite Member. Underlain by Nonning Rhyolite Member.||
79744|Yannabie Rhyolite Member|71317|2|Defined|p1, p20, p26-p27, p35-p36|Mesoproterozoic|Mesoproterozoic|Name derived from East Yannabie Dam. Type locality occurs 5km northeast of Paney (GDA94 561850, 6390300). Originally defined by Blissett, 1986 and 1987 as the Yannabie Rhyodacite before being retired by Allen et al., 2003; It is redefined here in this text as the Yannabie Rhyolite Member. Distribution discussed in detail. Where this unit intercalates with the Mount Friday Formation is an anomoalous zone of alteration and quartz-pyrite veining containing Ag, Pb, Cu, Mo, As, Bi and Sb. Has a reported thickness of approximately 100m. Referred to as the Yannabie Rhyolite on p58 and p69. See also p38, p49-p50, p54-p55, p58, p68, p69-p70, p73-p74-p75, p84, p156, p158, p191.|ca. 1587 Ma (CA-TIMS of parent)|Eucarro Rhyolite||Interbedded with the Paney Rhyolite Member. Overlain by the Pondanna Dacite Member and the Mount Friday Formation.|Reddish-brown, vesicular, porphyritic rhyolite containing phenocrysts of plagioclase, alkali feldspar, ferromagnesian phases and quartz in a fine grained groundmass.|
79744|Yannabie Rhyolite Member|71559|4|Described|p19|Mesoproterozoic|Mesoproterozoic|Geological province: Gawler Craton. ||Unit of Upper Gawler Range Volcanics.|||Rhyolite, red, amygdaloidal and porphyritic with phenocrysts of feldspar and abundant free quartz; vesicular top of flow.|19-JUN-19
79744|Yannabie Rhyolite Member|71560|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|||Eucarro Rhyolite.|||Rhyolite, red, amygdaloidal and porphyritic with phenocrysts of feldspar and abundant free quartz; vesicular top of flow.|
79744|Yannabie Rhyolite Member|72065|5|Briefly described|p105|Calymmian|Calymmian|Geological province: Gawler Craton.||Unit of Eucarro Rhyolite.||||
79744|Yannabie Rhyolite Member|72090|5|Briefly described|p12, p50, p59|||Gawler Craton.||Eucarro Rhyolite|||Dark grey to moderate reddish brown, porphyritic dacite with common quartz veining.|
79744|Yannabie Rhyolite Member|73110|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|||Eucarro Rhyolite.|||Rhyolite, amygdaloidal, vesicular, abundant free quartz; top of flow.|
79745|Yantea Rhyolite|70659|5|Briefly described|p6-8|Mesoproterozoic|Mesoproterozoic|||Glyde Hill Volcanic Complex.|||Rhyolite separated by volcaniclastic intervals of tuffaceous mudstone, crystal and pumice rich sandstone and breccia.|
79745|Yantea Rhyolite|70816|5|Briefly described|p5|||Lake Everard area, Gawler Ranges.||Unit of Glyde Hill Volcanic Complex.||Overlain by Whyeela Dacite. Underlain by Nuckulla Basalt.||
79745|Yantea Rhyolite|72090|6|Mentioned|p12|||Gawler Craton.||Glyde Hill Volcanic Complex||||
29217|Yapinga Ferricrete|22613|5|Briefly described|p25|Pleistocene|Oligocene|||||||
29217|Yapinga Ferricrete|22614|5|Briefly described|map|Tertiary|Tertiary|||||||
29217|Yapinga Ferricrete|40912|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
29217|Yapinga Ferricrete|44695|5|Briefly described|Map Legend||Tertiary|||||||
26243|Yarle Sandstone|22587|6|Mentioned|p79 Fig.7|Early Miocene|Early Miocene|||||||
26243|Yarle Sandstone|22613|4|Described|p21|Middle Miocene|Middle Miocene|||||||
26243|Yarle Sandstone|22614|5|Briefly described|map|Miocene|Miocene|||||||
26243|Yarle Sandstone|23488|6|Mentioned|p39|Miocene|Miocene|Geological Province: Eucla Basin.||||||
26243|Yarle Sandstone|24606|5|Briefly described|p957 Fig. 2|Early Pliocene|Middle Miocene|Geological Province: Eucla Basin||||||
26243|Yarle Sandstone|42086|5|Briefly described|Fig.2 P4|||||||||
26243|Yarle Sandstone|42265|2|Defined|p2|Miocene|Miocene|Occurs along the NE margin of the Nullarbor Plain - forming a narrow belt at the limit of the Nullarbor Limestone.  Exposures are silicified and ferruginised, usually in the floors and around margins of playa lakes. Age: Early to early Middle Miocene.||||||19-FEB-15
26243|Yarle Sandstone|42959|5|Briefly described|p58 Fig.3|||||||||
26243|Yarle Sandstone|44133|5|Briefly described|p184, 180 Fig. 10.22|Middle Miocene|Middle Miocene|Geological Province: Eucla Basin. Thickness: 10m. Silicified and ferruginous sandstone.||||||05-DEC-13
26243|Yarle Sandstone|44695|5|Briefly described|Map Legend|Miocene|Miocene|(Early-Middle Miocene)||||||
26243|Yarle Sandstone|64646|6|Mentioned|p23 Fig. 3, p24 Fig. 4|Miocene|Miocene|Geological Province: Eucla Basin.||||||08-FEB-10
26243|Yarle Sandstone|67462|5|Briefly described|Map legend.|Miocene|Miocene|Bunda Plateau, Eucla Basin.||||||
26243|Yarle Sandstone|68715|6|Mentioned|p30 Fig.5|Serravallian|Burdigalian|Bunda Plateau, Eucla Basin. ||||||
26243|Yarle Sandstone|69598|6|Mentioned|p9|Middle Miocene|Early Miocene|||||||
26243|Yarle Sandstone|69648|4|Described|p4, p6 Fig.3, p25-26, map legend|Miocene|Miocene|Source of sand for Tertiary coastal sand units. Age: Early to Middle Miocene. Colville Sandstone (of Lowry 1968, 1970) is a conceptually equivalent sediment in the NW part of Eucla Basin, but believed pre-Tertiary in age (Benbow, 1990b). Located around inner margin of Nullarbor Plain. Interpreted as being deposited in coastal environments. Type area is in vicinity of Yarle and Choolalie Lakes. Thickness: at least ~6 m (sands in LRWE Maralinga 14-17 drillholes to the north up to ~20 m thick, may be Yarle Sandstone).||Immarna Group||Sharply overlain by Nullarbor Limestone.|Coastal quartz sands and sandstones, v.fine-medium grained, commonly bimodal (small proportion well rounded,coarse-v.coarse quartz grains); rare pebble-sized limestone clasts; minor abraded skeletal remains (foraminifera, echinoids, algae, molluscs).|19-FEB-15
26243|Yarle Sandstone|73108|5|Briefly described|Map legend.|Pleistocene|Eocene||||||Sandstone, silicified and ferruginous. Contains rare clasts of Nullarbor Limestone and fossils.|
80472|Yartoo volcaniclastics""|71317|4|Described|p1, p20, p98-p104, p112, p86|Calymmian|Calymmian|Introduced in this volume as a new informal subunit of the Yardea Dacite. Only known from one sample collected by F. Radke of the Geological Survey of South Australia in 1979.||Yardea Dacite||Overlies the Pondanna Dacite Member. Overlain by the Moonaree Dacite Member.||04-APR-18
80472|Yartoo volcaniclastics""|71559|4|Described|p20-22|Mesoproterozoic|Mesoproterozoic|Geological province: Gawler Craton. New stratigraphic sub-unit of the Yardea Dacite (Werner et al., 2017c). Lithic clasts likely derived from underlying Pondanna Dacite Member. Deposited as pyroclastic or resedimented volcaniclastic deposits; fluvially reworked volcanic material.|||||Poorly-sorted, matrix-supported volcanic breccias containing disperes and variably altered feldspar crystals and vitriclasts; minor volcanic sandstones and siltstones.|19-JUN-19
27033|Yednalue Quartzite|22889|6|Mentioned|p31|Adelaidean|Adelaidean|Parent - Emeroo Subgroup.  Yednalue Quartzite of the Mid-North and Nackara Arc.||||||
27033|Yednalue Quartzite|23818|6|Mentioned|p59|||Equivalent of the Rhynie Sandstone.||||||
27033|Yednalue Quartzite|29780|6|Mentioned|p27|||Refs Spry 1952.||||||
27033|Yednalue Quartzite|30801|6|Mentioned|p5|||Torrensian. Table P5-6.||||||
27033|Yednalue Quartzite|30802|6|Mentioned|p7|||||||||
27033|Yednalue Quartzite|30807|6|Mentioned|p103|||Suggested map symbol||||||
27033|Yednalue Quartzite|32724|6|Mentioned|Fig.1|||Correlation. Torrensian||||||
27033|Yednalue Quartzite|32725|6|Mentioned|p3|||Refers Spry (1952). See also P4 & P6||||||
27033|Yednalue Quartzite|34535|6|Mentioned|p59|||Equiv. Rhynie Sst.||||||
27033|Yednalue Quartzite|35255|6|Mentioned|Fig.6|||||||||
27033|Yednalue Quartzite|35328|6|Mentioned|p9|||Tentative correlation with Bungaree Quartzite||||||
27033|Yednalue Quartzite|35904|6|Mentioned|Fig.2|||||||||
27033|Yednalue Quartzite|37461|6|Mentioned|Table 5.I|||||||||
27033|Yednalue Quartzite|37854|6|Mentioned|p15|||See also Table 1.||||||
27033|Yednalue Quartzite|38926|6|Mentioned|p31|||||||||
27033|Yednalue Quartzite|39348|6|Mentioned|Map legend|Adelaidean|Adelaidean|Torrensian||||||
27033|Yednalue Quartzite|39404|6|Mentioned|Map legend|Adelaidean|Adelaidean|Torrensian||||||
27033|Yednalue Quartzite|40225|6|Mentioned|Map sheet|||||||||
27033|Yednalue Quartzite|40294|3|Fully described|p34|||||||||
27033|Yednalue Quartzite|41404|3|Fully described|p84|||||||||
27033|Yednalue Quartzite|42222|6|Mentioned|Table 1 P5|||||||||
27033|Yednalue Quartzite|43052|5|Briefly described|p177|||||||||
27033|Yednalue Quartzite|60959|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Of the Emeroo Subgroup. White, medium to coarse grained feldspathic quartzite; siliceous siltstone.||||||
27033|Yednalue Quartzite|71237|14|Not recorded|p10, 19|||||||||
27033|Yednalue Quartzite|71240|14|Not recorded|p6, , p9-10, p19|||||||Correlated with Rhynie Sandstone.||
36882|Younger Granite Suite|23394|5|Briefly described|Map legend|Proterozoic|Proterozoic|||||||
36882|Younger Granite Suite|61523|5|Briefly described|p10|||See also "Younger Granite Suite". Geological Province: Mount Painter Inlier.||||||
36882|Younger Granite Suite|69019|6|Mentioned|p70.|||Of Coats and Blissett (1971), including Mudnawatana Granite and other intrusions in the Mt Babbage and Mt Painter Inliers.||||||
36882|Younger Granite Suite|69023|5|Briefly described|p74|||Of Coats and Blissett (1971), who grouped the Mudnawatana Granite of Bowes (1953) with various intrusions in the Mount Painter Inlier. It was subsequently revised by Teale (1979) who renamed the main unit the Mudnawatana Tonalite and limited it to outcrops in the Mount Babbage Inlier.||||||
30608|Younger Lincoln Supersuite|50605|5|Briefly described|p(i), 1.3, 5.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Gawler Craton & Curnamona Province. Age: 1757-1700Ma.||||||07-NOV-08
24601|Younghusband Conglomerate|22589|6|Mentioned|p129||Cryogenian|part of the Arkaroola Subgroup||||||
24601|Younghusband Conglomerate|22631|6|Mentioned|p177|||||||||
24601|Younghusband Conglomerate|23054|5|Briefly described|p10|||||||||
24601|Younghusband Conglomerate|23282|6|Mentioned|p51,54|||May be equivalent to Pindyin Sandstone.||||||
24601|Younghusband Conglomerate|23287|6|Mentioned|p102|||||||||
24601|Younghusband Conglomerate|23288|6|Mentioned|p128 Fig.5,18|||of Central and Eastern Officer Basin.||||||
24601|Younghusband Conglomerate|36733|2|Defined|p68|Adelaidean|Adelaidean|See also P23.  Basal Adelaidean.||||||
24601|Younghusband Conglomerate|37854|6|Mentioned|Table 1|||||||||
24601|Younghusband Conglomerate|38108|6|Mentioned|Table 1|||||||||
24601|Younghusband Conglomerate|38157|6|Mentioned|Table II|||||||||
24601|Younghusband Conglomerate|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Willouran||||||
24601|Younghusband Conglomerate|40294|6|Mentioned|Table 2|||||||||
24601|Younghusband Conglomerate|41403|3|Fully described|p48|||||||||
24601|Younghusband Conglomerate|42222|6|Mentioned|p11|||||||||
24601|Younghusband Conglomerate|42223|6|Mentioned|Fig.2 P36|||||||||
24601|Younghusband Conglomerate|43052|5|Briefly described|p172|||||||||
24601|Younghusband Conglomerate|44111|6|Mentioned|p.58 Fig. 2|||in Adelaide Geosyncline, presented as "Younghusband" only in Fig. 2.||||||
24601|Younghusband Conglomerate|44289|5|Briefly described|Map Legend||Neoproterozoic|||||||
24601|Younghusband Conglomerate|62453|5|Briefly described|p16|||Of the Callanna Group. Geological Province: Adeliade Rift Complex.||||||
24601|Younghusband Conglomerate|63397|6|Mentioned|5|||||||||
24601|Younghusband Conglomerate|63811|6|Mentioned|p523|||Possible equivalent of Pindyin Formation. Manya 5 borehole.||||||28-MAR-12
24601|Younghusband Conglomerate|64625|6|Mentioned|p246|||Basal clastic sediments of the Adelaide Rift Complex.|>c.830 Ma.|||||
24601|Younghusband Conglomerate|64793|6|Mentioned|p284 Fig.3|||Mentioned as Younghusband Conglomerate correlative (Fig.3) or equivalent (Fig.4), underlying Coominaree Dolomite correlative in the eastern Officer Basin.||||||
24601|Younghusband Conglomerate|64796|6|Mentioned|p183 fig 2, p185, p187, p190 Fig.8 |Neoproterozoic|Neoproterozoic|See also p193 Tb.1, p200 Fig.10. Of Adelaide Rift Complex. Outcrop very weathered.||Unit in Arkaroola Subgroup.||Is overlain by Coominaree Dolomite.|Includes dolomitic siltstone.|
24601|Younghusband Conglomerate|65365|5|Briefly described|p1, p6 Fig. 2 |Cryogenian|Cryogenian|Northern Adelaide Rift Complex. Misspelt as Youngusband Conglomerate in Fig.2.||||||
24601|Younghusband Conglomerate|67912|6|Mentioned|p26|||Acritarch occurrence mentioned. Possible equivalent of the Cryogenian-aged Pindyin Sandstone.||||||
82977|Yudnapinna Member|73227|4|Described|p26|Neoproterozoic|Neoproterozoic|Authors suggest this name as an elevation of Yudnapinna beds to recognize the unit as the basal member of the Whyalla Sandstone [soft proposal; not fully described/defined]. A type section is proposed in CSR Ltd drillhole PL 32 (SA Geodata drillhole 20720; 31o 27' 41""S, 137o 2' 27""E) between 163.00 and 212.25 m depth. Marioan.||Whyalla Sandstone||Underlain by Tapley Hill Formation. Conformably overlain by Whyalla Sandstone. Equivalent to Elatina Formation.|Red, green and grey-green siltstone and fine sandstone, with a carbonate matrix at many locations and contains abundant reddish lithic grains, which range from sand to small pebble size.|
68131|Yumba Formation|60707|5|Briefly described|p612 Fig. 1c|||On Flinders Island.||||||
24146|Yunta Well Leucogranite|22834|2|Defined|p39||Statherian|New formation name.||||||05-MAR-13
24146|Yunta Well Leucogranite|24197|5|Briefly described|p74 Tb. 8.1|Paleoproterozoic|Paleoproterozoic|Age: 1750-1700Ma.||||||07-FEB-11
24146|Yunta Well Leucogranite|41667|5|Briefly described|p36|||||||||
24146|Yunta Well Leucogranite|43052|5|Briefly described|Table 4.4|||Of Moody Suite.||||||18-AUG-08
24146|Yunta Well Leucogranite|50605|5|Briefly described|p(i), 1.3, 5.2, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Gawler Craton & Curnamona Province. Of the Moody Suite (Younger Lincoln Supersuite).||||||07-NOV-08
24146|Yunta Well Leucogranite|61070|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Variably foliated, medium to coarse-grained grey muscovite-tourmaline-bearing granite and pegmatite. Minor garnet. Geological Province: Gawler Craton.||||||12-JAN-10
24146|Yunta Well Leucogranite|65221|6|Mentioned|p30|Palaeoproterozoic|Palaeoproterozoic|of Moody Suite.||||||
24146|Yunta Well Leucogranite|65376|6|Mentioned|p83. |||Abundance of sedimentary xenoliths suggests mixing of Hutchison Group metasediments with lower crustal source material.||Unit in Moody Suite.||||
24146|Yunta Well Leucogranite|71862|4|Described|p7, p15, p17, p24, p36-p37, p39-p41, p43|||Forms a discrete, elliptical pluton 10km northwest of Tumby Bay. This unit has a weak foliation in the centre of the intrusion that grades to moderate around the margins suggesting late tectonic emplacement.||Moody Suite||Intrudes the Hutchison Group and the Sleaford Complex.|Medium- to coarse-grained, quartz-K feldspar-plagioclase=muscovite-garnet-biotite-tourmaline granite.|
36023|adamellite 36023|40911|6|Mentioned|Map legend||Mesoproterozoic|Porphyritic biotite adamellite, porphyritic hornblende-biotite adamellite and granite, porphyritic leucogranite and microgranite, and minor biotite granodiorite; pegmatite, aplite and quartz veins. K-Ar ages of 1031-1124Ma.||||||
36044|adamellite 36044|44535|6|Mentioned|map legend||Proterozoic|Unnamed unit used in Proterozoic Granites GIS. Desc: Biotite and hornblende adamellites.||||||
36024|charnockite 36024|23400|6|Mentioned|Map legend||Proterozoic|Unnamed unit used by Proterozoic Granites GIS. Unit is a subdivision of Hypersthene adamellites on Woodroffe 1967 1:250K map legend.||||||
36046|gneiss 36046|44535|6|Mentioned|map legend||Proterozoic|Unnamed unit used in Proterozoic Granites GIS. Desc: Gneissic pyroxene adamellites, gneissic granites, granitic gneisses, pyroxene granulites, pyroxene gneisses, amphibolites.||||||
36025|granite 36025|23400|6|Mentioned|Map legend||Proterozoic|Unnamed unit used by Proterozoic Granites GIS. Unit is a subdivision of Hypersthene adamellites on Woodroffe 1967 1:250K map legend.||||||
36045|microadamellite 36045|44535|6|Mentioned|map legend||Proterozoic|Unnamed unit used in Proterozoic Granites GIS. Desc: Micro adamellite, microgranite.||||||
31303|porphyritic veins and plugs 31303|39802|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
