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
21387|Burdunga Subgroup|44133|5|Briefly described|p178|Late Eocene|Middle Eocene|||||||
21387|Burdunga Subgroup|69648|5|Briefly described|p21|||Of Benbow et al. (1995a).||Immarna Group|Pidinga Formation, Hampton Sandstone, Ooldea Sand|||
21387|Burdunga Subgroup|73099|5|Briefly described|Map legend.|Eocene|Eocene|Meramangye and Tallaringa Palaeochannels.||Immarna Group.|Pidinga Formation.|Overlies Bulldog Shale (Marree Subgroup). Is overlain by Garford Formation.||
21395|Burrawing Amphibolite|23492|6|Mentioned|p8 Fig. 3.|||||||||
21395|Burrawing Amphibolite|23731|6|Mentioned|p21 Fig. 1.4|||||||||
21395|Burrawing Amphibolite|61070|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Middleback Subgroup. Fine to medium-grained hornblende-plagioclase amphibolite , interbedded gradationally with banded diopside-hornblende-rich calcsilicate gneiss, with minor calcite, epidote and tremolite. Geological Province: Gawler Craton.||||||12-JAN-10
21395|Burrawing Amphibolite|66302|6|Mentioned|p24|||||Hutchison Group||||
21425|Camelback Member|23322|4|Described|957 Fig.2, p966|Miocene|Oligocene|Middle part of the Gambier Limestone.  Geological Province: Gambier Basin.||||||07-SEP-09
21425|Camelback Member|44133|4|Described|p156|Early Miocene|Early Oligocene|Of the Gambier Limestone (Heytesbury Group). Geological Province: Gambier Basin. Thickness: 250m. Includes former Compton Conglomerate.||||||
21425|Camelback Member|50133|5|Briefly described|p3, p7, p9 Tb.1,  p11 Tb. 2|||Shown in tables as Gartners Calcarenite. Major & trace element geochemistry for 2 samples given||Of the Gambier Limestone|||Calcarenite limestone|
21425|Camelback Member|60785|5|Briefly described|p196.|Late Oligocene|Late Oligocene|Has yielded well-preserved fossil cetacean elements.||Of the Gambier Limestone.|||Pale cream-white porous bryozoal calcarenite.|
21425|Camelback Member|63124|3|Fully described|p87 Fig. 5.29, p92|Early Miocene|Early Oligocene|Of Gambier Limestone (Heytesbury Gp). Overlies Greenways Member, Gellibrand and Narrawaturk Marls, Dilwyn Formation and Sherbrook Group. May be overlain by Green Point Member or Bridgewater Fm. Age: ~32-~22Ma. Max.thickness: 250m. Geol.Prov: Gambier Basin||||||
21425|Camelback Member|69297|5|Briefly described|p79|Burdigalian|Chattian|Otway Basin.||Gambier Limestone||Unconformably overlies the Greenways Member. Overlain by the Green Point Member.|Sandy limestone.|
21425|Camelback Member|70077|5|Briefly described|Nelson: Fig.2. Regional: Fig.4|Miocene|Oligocene|Otway Basin: Gambier Embayment and Voluta Trough.||Gambier Limestone.||Overlies Greenways Member. Is overlain by Green Point Member.||
21425|Camelback Member|70078|5|Briefly described|Northern: Fig.2. Regional: Fig.4|Miocene|Oligocene|Gambier Embayment and Voluta Trough.||Gambier Limestone.||Overlies Greenways Member. Is overlain by Green Point Member.||
21555|Coonta Gabbro|22494|2|Defined|p34-35|Statherian|Statherian|||||||
21555|Coonta Gabbro|60953|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Gabbro, peridotite, diorite.||||||07-NOV-08
21555|Coonta Gabbro|61070|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Massive, coarse-grained, dark green gabbro. Includes massive, medium to coarse-grained dark green diorite and dark green-black, massive, coarse-grained peridotite. Geological Province: Gawler Craton.||||||12-JAN-10
21555|Coonta Gabbro|61108|5|Briefly described|map legend|Mesoproterozoic|Paleoproterozoic|Gabbro, peridotite, diorite.||||||07-NOV-08
21555|Coonta Gabbro|65376|6|Mentioned|p17. |Mesoproterozoic|Paleoproterozoic|||||||
21555|Coonta Gabbro|69048|6|Mentioned|p2|Mesoproterozoic|Mesoproterozoic|Southern Eyre Peninsula.||||||
21626|Dawson Hill Member|60959|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of the Lake Frome Group. Well rounded quartz arenite pebbles and cobbles.||||||
21626|Dawson Hill Member|68735|5|Briefly described|p236, p238|Middle Cambrian|Middle Cambrian|Jago et al. (2010). Paleocurrent data indicate a flow direction at about 010 degrees.||Upper unit of the Grindstone Range Sandstone.|||A basal 60 m of argillaceous poorly sorted feldspathic sandstone, overlain by a fine to medium-grained quartz-rich sandstone with abundant, extremely well-rounded cobbles and clasts, which are concentrated on the foresets of planar cross-beds.|10-APR-17
21626|Dawson Hill Member|68993|5|Briefly described|p543|Middle Cambrian|Middle Cambrian|~ 190 m thick in the type section.||Unit within the upper part of the Grindstone Range Sandstone.||||
21641|Depot Springs Subgroup|23211|6|Mentioned|Fig.2|||of Wilpena Group.||||||
21641|Depot Springs Subgroup|24586|5|Briefly described|p50 Fig. 1, p51 Fig. 1|Adelaidean|Adelaidean|Of the Wilpena Group (Heysen Supergroup). Includes Wearing Dolomite and the Wonoka Formation.  Geological Province: Adelaide Geosyncline.||||||05-JUL-06
21641|Depot Springs Subgroup|43845|5|Briefly described|Fig2 p42||Neoproterozoic|In Wilpena Group||||||12-JUL-16
21641|Depot Springs Subgroup|70406|6|Mentioned|p121,  Fig 5|||Unclear which, if any, of the units shown in Fig 5 are part of this Subgroup.||Of Wilpena Group. |Includes Wearing Dolomite, Wonoka Formation.|||
21641|Depot Springs Subgroup|70407|4|Described|p108-111, 112|Neoproterozoic|Neoproterozoic|Age: Ediacaran. Reference section designated in and adjacent to Patsy Springs canyon near Depot Springs H.S., 40 km east of Copley.||Of Wilpena Group.|Includes Wearing Dolomite, Wonoka Formation.|Unconformably overlies Aruhna Subgroup.||
21641|Depot Springs Subgroup|73222|6|Mentioned|p6|Ediacaran|Ediacaran|[Written as Depot Springs in Fig.2]. Adelaide Rift Complex.||Wilpena Group, Heysen Supergroup||||
21641|Depot Springs Subgroup|74367|6|Mentioned|p7 Fig.6, p8|Ediacaran|Ediacaran|||Wilpena Group||||
21902|Green Point Member|23322|4|Described|957 Fig.2, p966|Miocene|Oligocene|Chert nodules are rare.  Upper part of the Gambier Limestone.  Geological Province: Gambier Basin.||Gambier Limestone||||07-SEP-09
21902|Green Point Member|43667|6|Mentioned|Fig.3,p12||Early Miocene|||||||
21902|Green Point Member|44133|5|Briefly described|p156|Early Miocene|Early Miocene|Of the Gambier Limestone (Heytesbury Group). Geological Province: Gambier Basin. Thickness: 193m.||||||
21902|Green Point Member|63124|3|Fully described|p87 Fig. 5.29, p92-93|Middle Miocene|Early Miocene|Of Gambier Limestone (Heytesbury Gp). Overlies Camelback Member (Gambier Lst) conformably; also Greenways Member; unconformably overlain by Bridgewater and Coomandook Formations. Age: ~23 to at least 15.5Ma. Max. thickness: 193m. Geol.Prov: Gambier Basin.||||||31-JAN-08
21902|Green Point Member|69297|5|Briefly described|p79|Burdigalian|Burdigalian|Otway Basin.||Gambier Limestone||Overlies the Camelback Member. Overlain by the Narracoorle Limestone Member.|Sandy limestone.|
21902|Green Point Member|70077|5|Briefly described|Nelson: Fig.2. Regional: Fig.4|Miocene|Miocene|Otway Basin: Gambier Embayment and Voluta Trough.||Gambier Limestone.||Overlies Camelback Member. Is overlain by Naracoorte Limestone Member.||
21902|Green Point Member|70078|5|Briefly described|Northern: Fig.2. Regional: Fig.4|Miocene|Miocene|Gambier Embayment and Voluta Trough.||Gambier Limestone.||Overlies Camelback Member. Is overlain by Naracoorte Member.||
21910|Greenways Member|23322|4|Described|957 Fig.2, p966|Oligocene|Eocene|Contains abundant chert nodules.  Lower part of the Gambier Limestone.  Geological Province: Gambier Basin.||||||07-SEP-09
21910|Greenways Member|24202|5|Briefly described|p321|||Of the Gambier Limestone.  Geological Province: Gambier Sub-basin.||||||
21910|Greenways Member|43667|6|Mentioned|Fig.3,p12||Early Oligocene|||||||
21910|Greenways Member|44133|5|Briefly described|p156|Early Oligocene|Late Eocene|Of the Gambier Limestone (Heytesbury Group). Geological Province: Gambier Basin. Thickness: 70m.||||||
21910|Greenways Member|63124|3|Fully described|p87 Fig. 5.29, p91-92|Early Oligocene|Late Eocene|Of Gambier Limestone (Heytesbury Group). Unconformable over either Sherbrook Group or Dilwyn Formation; also conformably overlies Narrawaturk Marl. Conformably overlain by Camelback Member. Age: ~39.5-~32Ma. Thickness: ~128m. Geol.Prov: Gambier Basin.||||||31-JAN-08
21910|Greenways Member|69297|5|Briefly described|p79|Rupelian|Rupelian|Otway Basin.||Gambier Limestone||Overlies the Narrawaturk Marl. Unconformably overlain by the Camelback Member.|Sandy limestone.|
21910|Greenways Member|70077|5|Briefly described|Nelson: Fig.2. Regional: Fig.4|Oligocene|Oligocene|Otway Basin: Gambier Embayment and Voluta Trough.||Gambier Limestone.||Overlies Narrawaturk Marl. Is overlain by Camelback Member.||
21910|Greenways Member|70078|5|Briefly described|Northern: Fig.2. Regional: Fig.4|Oligocene|Oligocene|Gambier Embayment and Voluta Trough.||Gambier Limestone.||Overlies Narrawaturk Marl. Is overlain by Camelback Member.||
10001|Lady Don Quartzite|22631|6|Mentioned|p177|||||||||
10001|Lady Don Quartzite|22772|4|Described|p64,Table13.1|Cryogenian|Cryogenian|||||||
10001|Lady Don Quartzite|22857|5|Briefly described|p64, Tb. 13.1 (insert p70-71)|Willouran|Willouran|Of the Pintapah Subgroup (Poolamacca Group). White silicified quartzite. Max. thickness: 150m. Geological Province: Adeliade Fold Belt. See also p402 App. 1 Tb.A1.3.||||||25-JAN-08
10001|Lady Don Quartzite|30261|4|Described|Table 1|||Willouran age||||||
10001|Lady Don Quartzite|33004|6|Mentioned|p134|||||||||
10001|Lady Don Quartzite|34812|3|Fully described|p54|||||||||
10001|Lady Don Quartzite|35199|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
10001|Lady Don Quartzite|35692|6|Mentioned|p23|||||||||
10001|Lady Don Quartzite|36411|6|Mentioned|p269|||Refs Cooper et al. 1978 for definition.||||||
10001|Lady Don Quartzite|36733|6|Mentioned|Table 5|||||||||
10001|Lady Don Quartzite|37461|6|Mentioned|p335|||||||||
10001|Lady Don Quartzite|37854|6|Mentioned|Table 1|||||||||
10001|Lady Don Quartzite|37931|4|Described|p533|||||||||
10001|Lady Don Quartzite|38157|6|Mentioned|Table II|||||||||
10001|Lady Don Quartzite|39214|6|Mentioned|p5|||||||||
10001|Lady Don Quartzite|40294|6|Mentioned|Table 2|||||||||
10001|Lady Don Quartzite|40595|6|Mentioned|p91|||||||||
10001|Lady Don Quartzite|41403|4|Described|p48|||||||||
10001|Lady Don Quartzite|42222|6|Mentioned|p11|||||||||
10001|Lady Don Quartzite|42223|6|Mentioned|Fig.2 P36|||||||||
10001|Lady Don Quartzite|42531|5|Briefly described|Map legend|Adelaidean||||||||
10001|Lady Don Quartzite|42813|6|Mentioned|p14|||||||||
10001|Lady Don Quartzite|43265|5|Briefly described|Map Legend||Neoproterozoic|of Pintapah Subgroup.||||||
10001|Lady Don Quartzite|43268|5|Briefly described|Map Legend||Neoproterozoic|of Pintapah Subgroup.||||||
10001|Lady Don Quartzite|62724|5|Briefly described|p16|||Of Callanna Group in NSW. Mature quartz sandstone.||||||07-FEB-11
10001|Lady Don Quartzite|69023|6|Mentioned|p63|||||||||
10001|Lady Don Quartzite|69999|5|Briefly described|p21|||Appears as Lady Done Quartzite. On the Torrowangee and Fowlers Gap 1:100 000 sheet areas.|||||Metamorphic mineralogy includes chlorite and muscovite.|
10001|Lady Don Quartzite|70000|5|Briefly described|p34|Neoproterozoic|Neoproterozoic|||Unit in Pintapah Subgroup.|||Fluviatile to shallow marine, mature sandstone.|
10001|Lady Don Quartzite|70015|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Mineral deposits (if any) are shown.||Unit in Pintapah Subgroup.||Is overlain by Christine Judith Conglomerate.|Medium-grained, white, silicified quartzite.|
10001|Lady Don Quartzite|72461|6|Mentioned|p13, p16, p19|||||Pintapah Subgroup||||
10030|Laira Formation|12781|6|Mentioned|p386|Early Cretaceous|Early Cretaceous|Otway Basin. Maximum thickness 880m.||Crayfish Group.||Overlies Pretty Hill Formation. Is overlain by Katnook Sandstone.||
10030|Laira Formation|22686|5|Briefly described|Fig3p745,Table1p746|Barremian|Valanginian|Consists predominantly of shale, siltstone with minor fine-grained sandstone. Max Age: 134 Ma; Min Age: 123 Ma.  Geological Province: Otway Basin.||||||17-JAN-06
10030|Laira Formation|24208|5|Briefly described|p169|Early Cretaceous|Early Cretaceous|Of the Crayfish Group.  Geological Province: Penola Trough (Otway Basin).||||||
10030|Laira Formation|24209|5|Briefly described|p151|||Geological Province: Penola Trough (Otway Basin)||||||
10030|Laira Formation|24314|5|Briefly described|p61 Fig.2|Hauterivian|Valanginian|Geological Province: Otway Basin. Max. Thickness 890m. Of the Otway Supergroup.||||||30-NOV-04
10030|Laira Formation|24453|5|Briefly described|p809 Fig.2|Hauterivian|Valanginian|Of Crayfish Subgroup. Geological Province: Otway Basin.||||||07-FEB-11
10030|Laira Formation|24551|6|Mentioned|p245, 249|||Of the Crayfish Subgroup. Underlies: Katnook Sandstone.||||||
10030|Laira Formation|24562|5|Briefly described|p8 Fig. 2|Early Cretaceous|Early Cretaceous|Of the Crayfish Group.  Geological Province: Otway Basin.||||||
10030|Laira Formation|42361|2|Defined|p6|Barremian|Valanginian|||||||
10030|Laira Formation|42545|5|Briefly described|p18|||Otway Basin.||||||14-APR-08
10030|Laira Formation|42599|5|Briefly described|Fig.3 P614|||||||||
10030|Laira Formation|43171|6|Mentioned|5-8|||Age: 125-130 Ma||||||
10030|Laira Formation|43195|5|Briefly described|Map Legend||Early Cretaceous|See also commentary on back of map. Of Crayfish Group.||||||
10030|Laira Formation|43660|5|Briefly described|p14|||||||||
10030|Laira Formation|43733|6|Mentioned|Fig.2.11,p65||Early Cretaceous|||||||
10030|Laira Formation|43744|6|Mentioned|Fig.3,p3|||||||||
10030|Laira Formation|43747|5|Briefly described|p5||Early Cretaceous|||||||
10030|Laira Formation|43814|6|Mentioned|Fig.3,p115|||||||||
10030|Laira Formation|44133|5|Briefly described|p144|Hauterivian|Valanginian|Previously also known as 'Crayfish Group, Unit C'. Thickness: 863m.||||||
10030|Laira Formation|61017|5|Briefly described|p5 Fig. 2|Barremian|Hauterivian|Of the Crayfish Sungroup (Otway Group). Geological Province: Otway Basin.||||||07-FEB-11
10030|Laira Formation|61182|6|Mentioned|p12|||Of Morton (1990). Name assigned to fine-grained strata below Eumeralla Formation in South Australia only - equiv. of Geltwood Beach Formation in Victoria where it is not recognised.||||||
10030|Laira Formation|61470|5|Briefly described|p28 Fig. 5|Barremian|Hauterivian|Of the Crayfish Subgroup (Otway Group). Overlies Pretty Hill Formation; interfingers with Katnook Sandstone. Geological Province: Otway Basin.||||||12-OCT-05
10030|Laira Formation|61547|5|Briefly described|p459, p461, pp465-466, pp471-472. |Hauterivian|Valanginian|Forms the regional seal to the Pretty Hill Sandstone reservoir. Overbank to lacustrine deposits. Eroded and reworked material from this unit provided sediment for the Katnook Sandstone.||||Overlies the Pretty Hill Formation.|Consists of frequent, fine shale units: interbedded siltstones, shales and occasional sands.|
10030|Laira Formation|61622|5|Briefly described|p436 Fig. 2|Cretaceous|Cretaceous|Of Crayfish Group. Geological Province: Otway Basin.||||||07-FEB-11
10030|Laira Formation|61623|6|Mentioned|p449 Fig. 4|Early Cretaceous|Early Cretaceous|Of Crayfish Group. Geological Province: Otway Basin.||||||07-APR-09
10030|Laira Formation|61626|5|Briefly described|p486 Fig. 2|Early Cretaceous|Early Cretaceous|Of Crayfish Group. Geological Province: Otway Basin.||||||07-APR-09
10030|Laira Formation|61627|5|Briefly described|p500 Fig. 2|Early Cretaceous|Early Cretaceous|Of Crayfish Group. Underlain by Pretty Hill Formation. Geological Province: Otway Basin.||||||07-FEB-11
10030|Laira Formation|61628|5|Briefly described|p509 Fig. 3|Early Cretaceous|Early Cretaceous|Of Crayfish Subgroup. Geological Province: Otway Basin.||||||07-APR-09
10030|Laira Formation|63122|5|Briefly described|p17 Fig. 4.3||Hauterivian|Of the Crayfish Group. Max. thickness: 880m. Geological Province: Otway Basin.||||||
10030|Laira Formation|63124|3|Fully described|p48 Fig. 5.1, p49 Fig. 5.2, p63|Hauterivian|Valanginian|Of Morton (1990). Formerly unnamed in Pretty Hill Sandstone; also known as Geltwood Beach Member and Geltwood Beach Fm. Of Crayfish Gp. Overlies Pretty Hill Fm. Age: 136-125Ma. Max.thickness: 890m. Geological Province: Otway Basin. Shale/siltstone suite.||||||30-JAN-08
10030|Laira Formation|63125|5|Briefly described|p107, p116 Tb. 7.6|||Geological Province: Otway Basin. Mature for oil generation. Referred to as upper and lower Laira Formations.||||||
10030|Laira Formation|63129|5|Briefly described|p127|||Geological Province: Otway Basin.||||||30-JAN-08
10030|Laira Formation|63130|6|Mentioned|p141, p143|||Geological Province: Otway Basin. Its seal for the Pretty Hill Formation reservoirs is regionally thick - up to 900m.||||||31-JAN-08
10030|Laira Formation|63150|5|Briefly described|p96|||Geological province: Otway Basin. Microfasta evansii (non-marine algae) present in upper Foraminisporis wonthaggiensis Zone of this formation - probably representing maximum lake development.||||||
10030|Laira Formation|63267|5|Briefly described|p483, p485 Fig.2, p486, p490-491, p496|Early Cretaceous|Early Cretaceous|Main seal in the Penola Trough, Otway Basin. Floodplain to lacustrine deposits. Poor hydrocarbon source potential. Wireline log. Significance of faults discussed.||Crayfish Group.||Conformably and transitionally overlies Pretty Hill Formation. Is overlain by Katnook Sandstone.|Predominantly dark grey siltstone and shale, with thin, very fine-grained to granular sandstone and wispy shale interbeds.|
10030|Laira Formation|63269|5|Briefly described|p605|Early Cretaceous|Early Cretaceous|Otway Basin.||Crayfish Subgroup.||||
10030|Laira Formation|63431|5|Briefly described|p676, p677 Fig. 2|Hauterivian|Valanginian|Of Crayfish Group. Geological Province: Penola Trough/Otway Basin. See also p680.||||||07-FEB-11
10030|Laira Formation|66245|5|Briefly described|p6 Fig.5. |Barremian|Hauterivian|||Unit in Crayfish Subgroup.||Overlies Pretty Hill Formation. Is overlain by Katnook Sandstone.||
10030|Laira Formation|67367|5|Briefly described|p131 Fig.2, p132. |Barremian|Hauterivian|Is potentially generative for both oil and gas where it is thermally mature.||Unit in Crayfish Subgroup.||Conformably overlies the Pretty Hill Formation.||
10030|Laira Formation|67541|6|Mentioned|p76 Fig.1|||||||||
10030|Laira Formation|69297|5|Briefly described|p79, 104|Barremian|Hauterivian|Otway Basin.||Crayfish Subgroup||Overlies the Pretty Hill Formation. Overlain by the Katnook Sandstone.|Mudstone and shale.|06-SEP-18
10030|Laira Formation|69651|5|Briefly described|p10|Early Cretaceous|Early Cretaceous|||Crayfish Subgroup.||Overlies Pretty Hill Formation. Is overlain by Katnook Sandstone.||
10030|Laira Formation|69948|6|Mentioned|Fig.4.2|||Otway Basin (a rift basin). Sediment thickness, sonic log, gamma ray log all shown in contrast with Eromanga Basin (an intracratonic basin).||||Overlies Pretty Hill Formation. Is overlain by Katnook Sandstone.||
10030|Laira Formation|70077|5|Briefly described|Regional: Fig.4; p4, p8|Barremian|Hauterivian|Otway Basin: Robe-Penola Trough. Lower energy fluvial and lacustrine sediments. In SA, provides vertical and cross-fault sealing of Penola Trough gas reservoirs.||Crayfish Subgroup.||Overlies Pretty Hill Formation. Is overlain by Katnook Sandstone.||
10030|Laira Formation|70379|5|Briefly described|p717, p719, p723-729, p732|Early Cretaceous|Early Cretaceous|Otway Basin. Isopach map. 350-400m of sediments were subsequently eroded prior to deposition of Eumeralla Formation. Relationship of tectonic activity to sediment accumulation discussed in detail. Hauterivian to late Barremian.||Crayfish Group.||Overlies Pretty Hill Formation but is replaced by it in the E of the Basin. Is overlain unconformably by Eumeralla Formation.|Lacustrine and floodplain sediments.|
10030|Laira Formation|70880|6|Mentioned|p77|Barremian|Hauterivian|Otway Basin.||||||
10030|Laira Formation|71266|6|Mentioned|p614 Fig.3|Early Cretaceous|Early Cretaceous|Otway Basin.||||||
10030|Laira Formation|71342|6|Mentioned|Ch4 p9|||Otway Basin.||||||
10030|Laira Formation|72050|5|Briefly described|p233 Fig.2, 234-235, 238|Barremian|Hauterivian|Shales in this unit are well-developed seals.||Crayfish Group.|||Mainly lacustrine shales. Local interbedded sands and shales on basement highs.|
10030|Laira Formation|73356|6|Mentioned|p. v-1, p4, p10, p13-16, p20-21, p26-29|Barremian|Hauterivian|Otway Basin. Basal boundary with Pretty Hill Formation is gradational and may be diachronous.||Crayfish Subgroup, Otway Group||Underlain by Pretty Hill Formation. Overlain by and equivalent to Katnook Sandstone. Unconformably overlain by Windermere Sandstone.||
10030|Laira Formation|73357|6|Mentioned|p17|Barremian|Valangian|Otway Basin. Correlated to the Foraminisporis wonthaggiensis Zone, mid Valangian to mid Barremian age and with possible brackish influences.||||||
10030|Laira Formation|73383|5|Briefly described|p3, p7 Tb.3.1, p11, p15, p41-42, p62-64|Aptian|Valangian|Otway Basin. Equivalent to chemostratigraphic packages S1-P7 to S1-P9. Lithologies based on geochemistry using the ChemLith classification includes mudstone, limestone, argillaceous and calcareous sandstones, igneous rock, calcareous limestone and siltstone; and using the Herron classification (1988) includes shale, wacke, lith-arenite and Fe-shale. See also vi, p88-94, p100-102, p171, p194-195, p218-224, p229-231, p282, p285, p288-289, p292, p331, p333-334, p336, p339.||Crayfish Subgroup||Overlies Pretty Hill Formation, unconformably underlies Eumeralla Formation|Lacustrine mudstones and alluvial sandstones.|
10030|Laira Formation|73385|5|Briefly described|p5|Barremian|Valanginian|Otway Basin.||Crayfish Subgroup||Overlies Pretty Hill Formation, underlies Eumeralla Formation.|Lacustrine mudstones and alluvial sandstones.|
10030|Laira Formation|73386|4|Described|p4, p6, p8-9, Attachment A1|Barremian|Hauterivian|Otway Basin. Deposited in fluvial floodplain to shallow lacustrine environments. The formation is a thick shale unit in the Penola Trough, thins and becomes increasingly sandstone dominant along the northern basin margin towards the east. Primarily associated with the Upper Foraminisporis wonthaggiensis Spore-Pollen Subzone, corresponds to the S1-P7 to S1-P9 chemostratigraphic packages (Eid et al., 2021b). The interval from 1979 m to 2842 m in Katnook-2 is the designated type section.||Crayfish Subgroup||Overlies Pretty Hill Formation, unconformably underlies Eumeralla Formation, Windermere Sandstone, conformably underlies Katnook Sandstone in the west|Consists of light grey to green siltstone and claystone interbedded with fine grained sandstone.|
10030|Laira Formation|73594|5|Briefly described|p3-4, p42, p45 Fig.5.19, p47-48|Barremian|Valanginian|Otway Basin. Fluvial-lacustrine, deposited in alluvial floodplain and shallow lacustrine environments. Typically over 300 m thick, over 850 m thick in the type section at Katnook-2 well. Passes laterally into the Katnook Sandstone in the western part of the basin.||Crayfish Subgroup||Overlies Pretty Hill Formation, Pretty Hill Sandstone. Underlies Katnook Sandstone, Eumeralla Formation, Windemere Sandstone|Claystones, siltstones and minor sandstones. Includes massive, dissagregated shale with interbedded thin, quartzose sandstones at base.|
10041|Lake Dutton mudstone|38581|6|Mentioned|p259|||||||||
10045|Lake Frome Group|22631|6|Mentioned|p178|Cambrian|Cambrian|||||||
10045|Lake Frome Group|22766|4|Described|Fig.2 p561, p562|Middle Cambrian|Early Cambrian|See also p566.||||||09-OCT-06
10045|Lake Frome Group|22772|5|Briefly described|Table 13.1|Middle Cambrian|Middle Cambrian|||||||
10045|Lake Frome Group|22857|5|Briefly described|Tb 13.1 (insert p70-71), p90 Fig.14.7B|Late Cambrian|Middle Cambrian|Of the Morolana Supergroup [missp. of Moralana]. Age: 509-498Ma. Geological Province: Arrowie Basin. See also p92 and p404 App.1 Tb.A1.4.||||||04-MAY-10
10045|Lake Frome Group|22858|5|Briefly described|p92,Fig14.7bp90-1||Middle Cambrian|||||||
10045|Lake Frome Group|22949|5|Briefly described|p27|Middle Cambrian||Age max. - late Early Cambrian.||||||
10045|Lake Frome Group|23023|6|Mentioned|p1800|||||||||
10045|Lake Frome Group|23250|5|Briefly described|p1124 Fig.2|Late Cambrian|Middle Cambrian|Correlate of Pacoota Sandstone, Petermann Sandstone, Deception Sandstone, Illara Sandstone and Tempe Formation.||||||
10045|Lake Frome Group|23351|6|Mentioned|283|||||||||
10045|Lake Frome Group|23818|5|Briefly described|p51 Fig.16, p95|Late Cambrian|Middle Cambrian|Geological Province: Adelaide Geosyncline. Max. thickness: 12 000 ft.||||||18-APR-05
10045|Lake Frome Group|23981|5|Briefly described|p8-9 Fig. 4|Toyonian|Toyonian|Overlies Wirrealpa Limestone and Aroona Creek Limestone. Locally up to 2700m thick. Geological Province: Arrowie Basin.||||||
10045|Lake Frome Group|24138|5|Briefly described|p32|Cambrian|Cambrian|Red-brown micaceous shale, sandstone and thin dolomite beds. Geological Province: Adelaide Geosyncline.||||||
10045|Lake Frome Group|24176|3|Fully described|p17|Cambrian|Cambrian|Comprises Moodlatana Formation (lowermost), Balcoracana Fm., Pantapinna Sandstone and Grindstone Range Sandstone. Overlies Wirrealpa Limestone; underlies Balcoracana Fm.  Geological Province: Mount Painter Province.||||||25-JAN-08
10045|Lake Frome Group|24465|5|Briefly described|p345 Fig.2|Middle Cambrian|Early Cambrian|Includes  Grindstone Range and Pantapinna Sandstones and the Balcoracana and Moodlatana Formations.  Geological Province: Arrowie Basin.||||||19-JAN-05
10045|Lake Frome Group|29929|6|Mentioned|Fig.1|||||||||
10045|Lake Frome Group|30051|6|Mentioned|Fig.7|||See also Fig.12. Middle Cambrian age.||||||
10045|Lake Frome Group|30176|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
10045|Lake Frome Group|30544|6|Mentioned|p49|||Cambrian age||||||
10045|Lake Frome Group|30801|6|Mentioned|p5|||Middle Cambrian age. Table P5-6||||||
10045|Lake Frome Group|30802|4|Described|p11|||Cambrian age.||||||13-FEB-08
10045|Lake Frome Group|30917|6|Mentioned|p41|||||||||
10045|Lake Frome Group|30921|6|Mentioned|Map legend|Devonian|Devonian|||||||
10045|Lake Frome Group|31388|6|Mentioned|p549|||||||||
10045|Lake Frome Group|31797|6|Mentioned|Fig. 2|||M.Camb.||||||
10045|Lake Frome Group|31923|6|Mentioned|p11|||||||||
10045|Lake Frome Group|32343|6|Mentioned|Table 1|||||||||
10045|Lake Frome Group|32720|6|Mentioned|Table 1|||M.Cambrian.||||||
10045|Lake Frome Group|32722|6|Mentioned|Fig.3|||Camb. Stromatolite||||||
10045|Lake Frome Group|33474|6|Mentioned|Fig.3|||||||||
10045|Lake Frome Group|33738|6|Mentioned|p45|||||||||
10045|Lake Frome Group|33932|6|Mentioned|p14|||||||||
10045|Lake Frome Group|33934|6|Mentioned|Fig.2|||M - U Camb.||||||
10045|Lake Frome Group|33954|6|Mentioned|p97|||See also Fig.4||||||
10045|Lake Frome Group|33972|6|Mentioned|Fig.2|||||||||
10045|Lake Frome Group|34535|6|Mentioned|Fig.16|||Camb.||||||
10045|Lake Frome Group|34610|6|Mentioned|p178|||Middle - Upper Cambrian||||||
10045|Lake Frome Group|34612|6|Mentioned|p85|||See also p106. Correlation chart. Fig.33. Middle - Lower Cambrian||||||12-JUN-20
10045|Lake Frome Group|34812|6|Mentioned|Table 9|||||||||
10045|Lake Frome Group|35088|6|Mentioned|Fig.8|||||||||
10045|Lake Frome Group|35255|4|Described|p18|||||||||
10045|Lake Frome Group|35628|6|Mentioned|Table 3|||||||||
10045|Lake Frome Group|35798|6|Mentioned|Fig.4|||Correlation of lower units in Desert Syncline drill holes.||||||
10045|Lake Frome Group|35835|6|Mentioned|p209|||||||||
10045|Lake Frome Group|35954|6|Mentioned|p1230|||See also Fig.2.||||||
10045|Lake Frome Group|36083|6|Mentioned|p471|||||||||
10045|Lake Frome Group|36137|4|Described|p6|||||||||
10045|Lake Frome Group|36198|6|Mentioned|p249|||See also Fig.I.2.||||||
10045|Lake Frome Group|36495|6|Mentioned|Fig.1|||||||||
10045|Lake Frome Group|37461|6|Mentioned|p345|||||||||
10045|Lake Frome Group|37818|6|Mentioned|Table 2|||||||||
10045|Lake Frome Group|38004|6|Mentioned|p82|||||||||
10045|Lake Frome Group|38068|4|Described|p69|||See also Fig.4.||||||
10045|Lake Frome Group|38704|6|Mentioned|p133|||||||||
10045|Lake Frome Group|39344|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
10045|Lake Frome Group|39352|6|Mentioned|Map legend|Late Cambrian|Middle Cambrian|Middle to Late Cambrian||||||
10045|Lake Frome Group|40254|6|Mentioned|Fig.7|||||||||
10045|Lake Frome Group|40642|6|Mentioned|p172|||||||||
10045|Lake Frome Group|40852|6|Mentioned|p33|||||||||
10045|Lake Frome Group|40914|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
10045|Lake Frome Group|41401|6|Mentioned|p32|||||||||
10045|Lake Frome Group|41496|5|Briefly described|Fig.1|||||||||
10045|Lake Frome Group|41526|6|Mentioned|p3|||||||||
10045|Lake Frome Group|41810|6|Mentioned|p111|||||||||
10045|Lake Frome Group|42011|6|Mentioned|Fig.2 P457|||||||||
10045|Lake Frome Group|42090|6|Mentioned|p26|||||||||
10045|Lake Frome Group|42141|6|Mentioned|Table 2 P571|||||||||
10045|Lake Frome Group|42222|5|Briefly described|p11|||||||||
10045|Lake Frome Group|42239|6|Mentioned|Fig.2 p151|||||||||12-JUN-20
10045|Lake Frome Group|42240|6|Mentioned|Fig.2 p165|||||||||12-JUN-20
10045|Lake Frome Group|42269|4|Described|p337|||||||||
10045|Lake Frome Group|42272|6|Mentioned|Fig.2 P400|||||||||
10045|Lake Frome Group|42357|5|Briefly described|p10|||||||||
10045|Lake Frome Group|42573|5|Briefly described|Fig.1 P190|||||||||
10045|Lake Frome Group|43011|6|Mentioned|Table 2,p12|||||||||
10045|Lake Frome Group|43053|5|Briefly described|Map Legend|Cambrian|Cambrian|Shallow marine to terrestrial redbeds, peritidal to marine limestone.||||||25-MAY-05
10045|Lake Frome Group|43258|5|Briefly described|Map Legend||Cambrian|||||||
10045|Lake Frome Group|43298|6|Mentioned|Map Legend||Cambrian|||||||
10045|Lake Frome Group|43595|6|Mentioned|p545||Cambrian|||||||
10045|Lake Frome Group|44093|5|Briefly described|p138 App. 1|Middle Cambrian|Early Cambrian|Geological Province: Adelaide Fold Belt.||||||
10045|Lake Frome Group|44133|5|Briefly described|p28, 46|Late Cambrian?|Middle Cambrian|Maximum Thickness: 2700m.||||||
10045|Lake Frome Group|45155|6|Mentioned|Fig.8|||||||||
10045|Lake Frome Group|60718|5|Briefly described|p48 Fig. 1|Cambrian|Cambrian|Geological Province: Adelaide Geosyncline.||||||13-FEB-08
10045|Lake Frome Group|60889|4|Described|p247-9|Middle Cambrian|Early Cambrian||<512 Ma||Moodlatana Formation, Balcoracana Formation, Pantapinna Sandstone, Grindstone Range Sandstone||Thick succession of red-brown siliciclastics that is marginal marine at base and fluvial at top.|
10045|Lake Frome Group|60953|5|Briefly described|Map Legend|Cambrian|Cambrian|Geological Province: Arrowie Basin.||||||27-APR-05
10045|Lake Frome Group|60959|5|Briefly described|Map Legend|Middle Cambrian|Early Cambrian|Of the Moralana Supergroup.||||||
10045|Lake Frome Group|61108|5|Briefly described|map legend|Cambrian|Cambrian|Shallow marine to terrestrial redbeds; peritidal to marine limestone. Geological Province: Arrowie Basin.||||||03-JUN-05
10045|Lake Frome Group|62592|5|Briefly described|p20 Fig.2.4, p50 Table 5.1, p59.|||Colour scheme shown for interpretation of Curnamona seismic sections. Thickness of 2.7 km in eastern Flinders Ranges.||Unit in Moralana Supergroup.|Includes Moodlatana and Balcoracana Formations, and Pantapinna and Grindstone Range Sandstones.|Overlies Wirrealpa Limestone.|Redbed clastics.|
10045|Lake Frome Group|62724|5|Briefly described|p22|Cambrian|Cambrian|Geological Province: Adelaide Geosyncline.||||||07-FEB-11
10045|Lake Frome Group|62742|5|Briefly described|p699 Fig. 2|Ordovician|Cambrian|Quartz-rich sandstone, conglomerate and mudstone.||||||
10045|Lake Frome Group|62744|5|Briefly described|p709 Fig. 2|Ordovician|Cambrian|||||||
10045|Lake Frome Group|62784|5|Briefly described|p8 Fig.1|Cambrian|Cambrian|Arrowie Basin. Includes Moodlatana Formation. Overlies Wirrealpa Limestone.||||||
10045|Lake Frome Group|63569|6|Mentioned|pp117-118|Middle Cambrian|Early Cambrian|Arrowie Basin.|||Includes Moodlatana and Balcoracana Formations, and Pantapinna and Grindstone Range Sandstones.|||
10045|Lake Frome Group|65313|6|Mentioned|p578 Fig. 6|Ordovician|Cambrian|Flinders Ranges area.|||Includes Moodlatana Formation, Balcoracana Formation, Pantapinna Sandstone, Grindstone Range Sandstone.|Overlies Wirrealpa Limestone.||26-MAR-12
10045|Lake Frome Group|65375|5|Briefly described|p33.|Cambrian|Cambrian||||Includes Moodlatana and Balcoracana Formations; Pantapinna and Grindstone Range Sandstones.|||
10045|Lake Frome Group|65625|5|Briefly described|p103 Fig.2|Middle Cambrian|Middle Cambrian|Lake Frome area.|||Includes Moodlatana Formation, Balcoracana Formation, unnamed sandstone, and Grindstone Range Sandstone.|Overlies Wirrealpa Limestone.||13-APR-11
10045|Lake Frome Group|65892|5|Briefly described|p9 Fig.4, p11, p38, p41, p49. |Middle Cambrian|Early Cambrian|Arrowie Basin. A thick succession of red-brown siliciclastics, marginal marine at the base and fluvial at the top.|||Includes Moodlatana and Balcoracana Formations, Grindstone Range and Pantapinna Sandstones.|||
10045|Lake Frome Group|65925|5|Briefly described|p14 Fig.2.2, Appendix 2.|Middle Cambrian|Early Cambrian||||Includes Moodlatana and Balcoracana Formations and Pantapinna and Grindstone Range Sandstones.||Sandstone, siltstone, shale, limestone, conglomerate.|
10045|Lake Frome Group|66518|5|Briefly described|p19 Fig.4.|Cambrian|Cambrian|Arrowie Basin.|||Includes Moodlatana and Balcoracana Formations, and Pantapinna and Grindstone Range Sandstones.|Overlies Wirrealpa Limestone.||
10045|Lake Frome Group|67030|6|Mentioned|p412 Fig. 7||Cambrian|Magnetic information presented for comparison. Abbreviated as Lake Frome Gp. (basal).||||||26-APR-12
10045|Lake Frome Group|67536|5|Briefly described|Map Legend|Stage 2|Stage 2||ca. 523 +/- 2 Ma||||Shallow marine to terrestrial redbeds, peritidal to marine limestone|
10045|Lake Frome Group|67870|5|Briefly described|p5, p9, p15, p17, p23-25|Cambrian|Cambrian|Arrowie Basin. Appears also as Wirrealpa-Lake Frome Group on p25.|||||Sandstone, siltstone, limestone.|
10045|Lake Frome Group|68030|6|Mentioned|p239|Cambrian|Cambrian|Flinders Ranges.||||Underlain by Wirrealpa Limestone.||
10045|Lake Frome Group|68068|5|Briefly described|Map legend|Cambrian|Cambrian|Arrowie Basin. Known only from SANTOS CBH-2. Sandy shoreface-shallow subtidal environment with some sub-aerial exposure.|||Includes Pantapinna Formation.||Red bed sequence; feldspathic flat to cross-bedded sandstone-mudstone, planar reactivation surfaces common, mudcracks and local bioturbation zones; diagenetic red mottling and green reduction patches.|13-NOV-14
10045|Lake Frome Group|68314|5|Briefly described|p754|Middle Cambrian|Early Cambrian||||||Quartz-rich sandstone, conglomerate and mudstone.|
10045|Lake Frome Group|68713|6|Mentioned|p19|Middle Cambrian|Middle Cambrian|||||||
10045|Lake Frome Group|68735|5|Briefly described|p231, p233-239|Middle Cambrian|Early Cambrian|Arrowie Basin. Clastic sediments derived from the Gawler Craton.|||Includes Grindstone Range Sandstone, Pantapinna Sandstone, Balcoracana Formation, and Moodlatana Formation.|Underlain by the Wirrealpa Limestone.|Clastic-dominated succession.|10-APR-17
10045|Lake Frome Group|68993|5|Briefly described|p543, p544 Fig.1|Middle Cambrian|Early Cambrian|Arrowie Basin. Reliable paleontological evidence is provided by the trilobite Onaraspis rubra within the top part of the Moodlatana Formation (Jell in Bengtston et al. 1990).|||Includes Grindstone Range and Pantapinna Sandstones; Balcoracana and Moodlatana Formations.|||28-JUL-15
10045|Lake Frome Group|69019|5|Briefly described|p66, p69-70, p144, p172 Fig.40.|Middle Cambrian|Middle Cambrian|Subsurface only in this map area. Possible Pantapinna Formation equivalent. Undeformed in this map area.|||||Red-beds: feldspathic sandstone and interbedded mudstone.|
10045|Lake Frome Group|69023|5|Briefly described|p81, p166|Cambrian|Cambrian|A sandy shoreline to shallow subtidal environment with some subaerial exposure is deduced. Age is tentative because of lack of fossils. Possible equivalent of Pantapinna Formation. Has a geothermal exploration well (Yerila 1) terminating at 693m. Appears as Frome Group on p166.|||||Red-bed sequence: feldspathic, flat-bedded to cross-bedded sandstone to mudstone. Mud cracks, local bioturbation zones, diagenetic red mottling and green reduction zones, and one presumed trilobite trail occur.|
10045|Lake Frome Group|69982|6|Mentioned|p40, p42|Middle Cambrian|Middle Cambrian|Mentioned in the context of dating the Innamincka Formation by trilobite tracks similar to those in this unit, and similar lithologies with an informal sandstone.||||||
10045|Lake Frome Group|70031|6|Mentioned|p250|||487+\-5 Ma date for late Cryogenian to post-Delamerian Orogeny poles. See p250 Table 2 for paleomagnetic analysis.||||||
10045|Lake Frome Group|70790|6|Mentioned|p258|Middle Cambrian|Middle Cambrian||~510-505 Ma.|||||
10045|Lake Frome Group|70835|6|Mentioned|p335|Cambrian|Cambrian|Arrowie Basin, Flinders Ranges.|||Moodlatana Formation.|||
10045|Lake Frome Group|72429|6|Mentioned|p973, p976-977|||||||||
10045|Lake Frome Group|72449|6|Mentioned|p1|||Shallow water sediments. ?Correlated with Billy Creek Formation.||||||
10045|Lake Frome Group|73251|6|Mentioned|p36|||Arrowie Basin, Moorowie and Yalkalpo Sub-basins. Thermally late to post-mature.|||Grindstone Range Sandstone, Pantapinna Sandstone, Balcoracana Formation, Moodlatana Formation|Underlain by Wirrealpa Limestone.||
10081|Lakes Entrance Formation|13323|5|Briefly described|p393 Fig. 2|Late Oligocene|Early Oligocene|Of the Latrobe Valley Subgroup (Seaspray Group). Marine carbonates. Geological Province: Gippsland Basin.||||||
10081|Lakes Entrance Formation|13324|5|Briefly described|p94 Fig. 4, Fig. 10|Miocene|Oligocene|Gippsland Basin.||Of Seaspray Group||||
10081|Lakes Entrance Formation|13332|5|Briefly described|p184 Fig.2|Miocene|Oligocene|Geological Province: Gippsland Basin.||||||
10081|Lakes Entrance Formation|13350|5|Briefly described|p94, p96 Fig.3|Miocene|Oligocene|Of the Seaspray Group. Geological Province: Gippsland Basin.  See also p100 Fig. 7.||||||30-JUN-06
10081|Lakes Entrance Formation|22663|5|Briefly described|V97 - G1 to G4 Fig.2|Miocene|Miocene|||||||01-MAR-10
10081|Lakes Entrance Formation|23230|5|Briefly described|Table4-1p40||Oligocene|||||||
10081|Lakes Entrance Formation|23372|4|Described|p250,251 Fig.3|Oligocene|Eocene|Of Gippsland Basin.||||||01-JUL-08
10081|Lakes Entrance Formation|23768|5|Briefly described|p28 Fig.5|Early Miocene|Oligocene|Geological Province: Gippsland Basin.  See also p125 Fig. 42.||||||29-MAR-05
10081|Lakes Entrance Formation|23885|6|Mentioned|p163 Fig 14.3|||Geological Province: Gippsland Basin.||||||
10081|Lakes Entrance Formation|23909|5|Briefly described|p290 Fig.3|Miocene|Miocene|Of Seaspray Group.  Geological Province: Gippsland Basin.||||||
10081|Lakes Entrance Formation|24038|5|Briefly described|p439 Fig.2|Oligocene|Oligocene|Geological Province: Gippsland Basin||||||
10081|Lakes Entrance Formation|24053|4|Described|p37|Oligocene|Oligocene|Of Seaspray Group.  Max. thickness: 91m.  Geological Basin: Gippsland Basin.||||||
10081|Lakes Entrance Formation|24054|4|Described|p46|||Geological Province: Gippsland Basin.||||||30-AUG-06
10081|Lakes Entrance Formation|24090|5|Briefly described|p8 Fig.3|Oligocene|Oligocene|Geological Province: Gippsland Basin.||||||
10081|Lakes Entrance Formation|24164|5|Briefly described|p11,18,20,22,29,30,32,37,40 and more|Miocene|Oligocene|Horizon top of this unit was mapped from seismic data. Presented as Lakes Entr. Formation in Fig.12. Included in Figs.10,12,14,19,22,26.||Seaspray Group||Is overlain by Gippsland Limestone Formation; overlies Latrobe Group||
10081|Lakes Entrance Formation|24211|5|Briefly described|p86 Fig. 3|Miocene|Oligocene|Marine marls, claystones and carbonates.  Geological Province: Gippsland Basin.  See also p85 Fig. 2 and p87 Fig. 4.||||||
10081|Lakes Entrance Formation|24403|5|Briefly described|p3|||Geological Province: Gippsland Basin.||||||
10081|Lakes Entrance Formation|24405|6|Mentioned|p5|||Geological Province: Gippsland Basin.||||||12-AUG-04
10081|Lakes Entrance Formation|24407|5|Briefly described|p13 Fig.2|Oligocene|Oligocene|Geological Province: Gippsland Basin.||||||01-JUL-08
10081|Lakes Entrance Formation|24495|6|Mentioned|p9, p10|||Marls.  Geological Province: Gippsland Basin.||||||
10081|Lakes Entrance Formation|24551|5|Briefly described|p262 Fig. 9.29, p327 Fig. 10.33|Miocene|Oligocene|Of the Seaspray Group.||||||
10081|Lakes Entrance Formation|24561|5|Briefly described|p44|Oligocene|Oligocene|Geological Province: Gippsland Basin. Basal unit of the basin. Predominantly marl.||||||04-FEB-08
10081|Lakes Entrance Formation|29500|6|Mentioned|p11|||||||||
10081|Lakes Entrance Formation|29591|5|Briefly described|p98|||||||||
10081|Lakes Entrance Formation|29650|6|Mentioned|p111|||||||||
10081|Lakes Entrance Formation|29678|6|Mentioned|p191|||||||||
10081|Lakes Entrance Formation|29721|6|Mentioned|p192|||||||||
10081|Lakes Entrance Formation|29736|6|Mentioned|Fig.2|||||||||
10081|Lakes Entrance Formation|29974|6|Mentioned|p47|||||||||
10081|Lakes Entrance Formation|30836|4|Described|p1264|||Oligcene||||||
10081|Lakes Entrance Formation|30933|6|Mentioned|Map legend|Oligocene|Eocene|Eocene-Miocene||||||
10081|Lakes Entrance Formation|31159|6|Mentioned|p85|||See also P86, 87, 88.||||||
10081|Lakes Entrance Formation|31351|5|Briefly described|Fig. 5|||See also P85, 87||||||
10081|Lakes Entrance Formation|31352|4|Described|p133|||See also P137, Fig. 3. Oligocene.||||||
10081|Lakes Entrance Formation|31480|4|Described|p74|||Oligocene - Miocene||||||
10081|Lakes Entrance Formation|31508|6|Mentioned|Table 1|||Oligocene||||||
10081|Lakes Entrance Formation|31627|6|Mentioned|p12|||||||||
10081|Lakes Entrance Formation|31646|6|Mentioned|Fig. 2|||||||||29-SEP-04
10081|Lakes Entrance Formation|31850|6|Mentioned|p36|||Refers Carter (1964)||||||
10081|Lakes Entrance Formation|31922|6|Mentioned|p166|||||||||
10081|Lakes Entrance Formation|32574|6|Mentioned|p77|||||||||
10081|Lakes Entrance Formation|32679|6|Mentioned|p94|||||||||
10081|Lakes Entrance Formation|33130|6|Mentioned|p60|||||||||
10081|Lakes Entrance Formation|33267|6|Mentioned|p70|||See also Fig.8||||||
10081|Lakes Entrance Formation|33320|6|Mentioned|p57|||Olig. Mioc.||||||
10081|Lakes Entrance Formation|33362|6|Mentioned|p112|||||||||
10081|Lakes Entrance Formation|33459|6|Mentioned|Table 1|||||||||
10081|Lakes Entrance Formation|33929|6|Mentioned|p70|||See also PP71 - 73.||||||
10081|Lakes Entrance Formation|34519|5|Briefly described|p46|||||||||
10081|Lakes Entrance Formation|34558|4|Described|p19|||See also Fig.2||||||
10081|Lakes Entrance Formation|34842|4|Described|p21|||||||||
10081|Lakes Entrance Formation|34843|6|Mentioned|p10|||||||||
10081|Lakes Entrance Formation|34954|6|Mentioned|Fig.35|||||||||
10081|Lakes Entrance Formation|35013|5|Briefly described|p397|||||||||
10081|Lakes Entrance Formation|35067|6|Mentioned|Fig.3|||||||||
10081|Lakes Entrance Formation|35273|3|Fully described|p257|||||||||
10081|Lakes Entrance Formation|35285|6|Mentioned|p415|||||||||
10081|Lakes Entrance Formation|35573|6|Mentioned|Fig.3|||Chronostratigraphic section - Gippsland Basin||||||
10081|Lakes Entrance Formation|36107|6|Mentioned|p101|||||||||
10081|Lakes Entrance Formation|36310|6|Mentioned|p149|||||||||
10081|Lakes Entrance Formation|36331|6|Mentioned|Fig.1|||See also P24||||||
10081|Lakes Entrance Formation|36643|6|Mentioned|Fig.7|||||||||
10081|Lakes Entrance Formation|36916|6|Mentioned|p107|||||||||
10081|Lakes Entrance Formation|37127|6|Mentioned|p349|||||||||
10081|Lakes Entrance Formation|37330|5|Briefly described|Table 4|||||||||
10081|Lakes Entrance Formation|37530|3|Fully described|p9|||||||||
10081|Lakes Entrance Formation|37783|6|Mentioned|Fig.12|||||||||
10081|Lakes Entrance Formation|37809|6|Mentioned|p7|||||||||
10081|Lakes Entrance Formation|38070|6|Mentioned|Fig.12|||Gippsland Basin||||||
10081|Lakes Entrance Formation|38313|6|Mentioned|Fig.2|||||||||
10081|Lakes Entrance Formation|38422|6|Mentioned|p151|||||||||
10081|Lakes Entrance Formation|38739|5|Briefly described|p285|||||||||
10081|Lakes Entrance Formation|38929|4|Described|p48|||See also Fig.6||||||
10081|Lakes Entrance Formation|38930|6|Mentioned|p59|||Also mentioned Fig.1||||||
10081|Lakes Entrance Formation|38973|6|Mentioned|p565|||||||||
10081|Lakes Entrance Formation|39446|5|Briefly described|p56|||||||||
10081|Lakes Entrance Formation|40716|5|Briefly described|p67|||||||||
10081|Lakes Entrance Formation|41171|6|Mentioned|p166|||||||||
10081|Lakes Entrance Formation|41193|6|Mentioned|p315|||||||||
10081|Lakes Entrance Formation|41213|5|Briefly described|Fig.2|||||||||
10081|Lakes Entrance Formation|41227|6|Mentioned|p4|||||||||
10081|Lakes Entrance Formation|41259|6|Mentioned|Fig.4|||||||||
10081|Lakes Entrance Formation|41282|6|Mentioned|p34|||||||||
10081|Lakes Entrance Formation|41534|5|Briefly described|p12|||||||||
10081|Lakes Entrance Formation|41537|6|Mentioned|Fig.2|||||||||
10081|Lakes Entrance Formation|41727|5|Briefly described|p433|||||||||
10081|Lakes Entrance Formation|41868|5|Briefly described|p522|||||||||
10081|Lakes Entrance Formation|42083|4|Described|Fig.9 P346|||||||||
10081|Lakes Entrance Formation|42311|5|Briefly described|Fig.2 P526|||||||||
10081|Lakes Entrance Formation|42649|6|Mentioned|Fig.6 P203|||of Seaspray Group||||||
10081|Lakes Entrance Formation|42827|3|Fully described|p331|||Of Seaspray Group.||||||12-FEB-08
10081|Lakes Entrance Formation|43145|4|Described|p11,p69||Early Oligocene|Of Seaspray Group.||||||12-FEB-08
10081|Lakes Entrance Formation|43667|6|Mentioned|Fig.3,p12||Miocene|||||||
10081|Lakes Entrance Formation|48631|5|Briefly described|p4,5,6,Pl.1,sh2||Oligocene|(J/55-11).||||||
10081|Lakes Entrance Formation|48636|4|Described|p.14,15,17,19,60|||(J55-11/Sale).||||||
10081|Lakes Entrance Formation|60538|5|Briefly described|p475 Fig. 14, 482 Fig. 21|Oligocene|Oligocene|Geological Province: Gippsland Basin. Of the Seaspray Group.||||||
10081|Lakes Entrance Formation|60666|5|Briefly described|p15 (Fig.)|||Geological Province: Gippsland Basin.||||||
10081|Lakes Entrance Formation|61155|5|Briefly described|p18|Middle Miocene|Late Eocene|Of the Seaspray Group. Fine-grained deep-water marls and carbonates. Overlies the Latrobe Group (Gurnard Formation); overlain by Gippsland Limestone. Thickness: 500m (offshore). Geological Province: Gippsland Basin (offshore). See p3, p8.||||||01-JUL-08
10081|Lakes Entrance Formation|61212|5|Briefly described|p301 Fig. 2|Miocene|Early Oligocene|Geological Province: Gippsland Basin.||||||
10081|Lakes Entrance Formation|61302|5|Briefly described|p5, p12|||Of Seaspray Group. Consists of a basal sand and gravel member, a glauconitic sandstone member, a micaceous marl member and an interbedded marl limestone member. Overlies Latrobe Group. Caps the Cunningham Greensand Member. Geol. Prov: Gippsland Basin.||||||02-JUN-06
10081|Lakes Entrance Formation|61323|5|Briefly described|p3 Fig. 3|Miocene|Oligocene|Geological Province: Gippsland Basin.||||||
10081|Lakes Entrance Formation|61329|6|Mentioned|p130|||||||||
10081|Lakes Entrance Formation|61336|5|Briefly described|p(iv) Fig. 4|Late Oligocene|Late Oligocene|Of the Seaspray Group. Disconformably overlies Latrobe Group. Geological Province: Gippsland Basin. See also p(v) Fig. 5.||||||07-FEB-11
10081|Lakes Entrance Formation|61469|5|Briefly described|p33|||Overlies Gurnard Formation. Geological Province: Gippsland Basin.||||||12-OCT-05
10081|Lakes Entrance Formation|61552|6|Mentioned|p583 Fig.2. |Late Oligocene|Early Oligocene|||Unit in Latrobe Valley Subgroup.||||
10081|Lakes Entrance Formation|61627|6|Mentioned|p504|||Geological Province: Gippsland Basin.||||||07-FEB-11
10081|Lakes Entrance Formation|62899|5|Briefly described|p37 Fig. 2|||Includes Cunningname (misspelling?) Greensand Member and Metung Marl Member. Geological province: Lakes Entrance Platform.||||||12-DEC-06
10081|Lakes Entrance Formation|63173|5|Briefly described|p342 Fig. 9.2|Middle Miocene|Early Oligocene|Geological Province: Gippsland Basin, offshore. Regional sealing unit for underlying hydrocarbon traps in this basin. Correlates with uppermost Demons Bluff  Formation in the Bass Basin.||||||07-FEB-11
10081|Lakes Entrance Formation|63739|5|Briefly described|p37 Fig. 2|||Includes Colquhoun Sandstone, Cunningname Greensand and Metung Marl Members. Overlain by Gippsland Limestone. Geological province: Gippsland Basin.||||||
10081|Lakes Entrance Formation|64876|5|Briefly described|p145 Fig.2|Oligocene|Oligocene|Gippsland Basin.||Seaspray Group.||||
10081|Lakes Entrance Formation|65717|5|Briefly described|p4-7, p9 Fig.2.2, p11-17, p19-28, p30-34|Oligocene|Oligocene|See also p38; Appendix 1, 3. Considered to be a high quality regional top seal for CO2 containment, and one of the most important in the Gippsland Basin. Thickness (from 19m to 430m) and depth to basement (400m to 3,500m) increase offshore. MICP anlaysis results. Top, base, thickness from named offshore wells tabulated.||Basal Latrobe Valley Subgroup.|Cunningham Greenstone Member, Giffard Sandstone Member, Colquhoun Sandstone Member, Seacombe Marl, Metung Marl.|Unconformably overlies Burong, Gurnard Formations. Is overlain by Gippsland Limestone.|Thick calcareous mudstones, shales interbedded with marl and glauconite.|05-SEP-17
10081|Lakes Entrance Formation|65718|5|Briefly described|p4, p5, p10 Fig 3.2, p12, p18, pp22-26|Miocene|Oligocene|Hocking (1976). Gippsland Basin. Considered a basin-wide, high quality regional top seal to the oil and gas accumulations at the top Latrobe Group reservoirs. Early Miocene minimum age.||Basal unit of the Seaspray Group.|Includes the Cunninghame Greensand Member, Giffard Sandstone Member (basal unit), Colquhoun Sandstone Member, Seacombe Marl Member, and Metung Marl Member.|Overlain by the Gippsland Limestone and the Haunted Hills Formation. Interfingers with the Balook Formation.|Composed predominantly of smectite-rich calcareous mudstones and claystones, with some variation in composition across the basin.|10-JAN-17
10081|Lakes Entrance Formation|65973|5|Briefly described|p17, p21-22, p33, p57, p62, p65, p71|Oligocene|Oligocene|Gippsland Basin. Forms a  high-quality regional seal to oil and gas accumulations in the Latrobe interval. Varies in thickness from 100m to over 300m in deeper parts of the basin. Geophysical response is discussed briefly. Intersected in Kipper-1, Judith-1, Hammerhead-1, East Pilchard-1, Longtom-1, Longtom-1/ST-1, Northright-1, Sole-1, Sweep-1 and many more drillholes (see appendix). See also p74, p76-77, p78, p80, p82, p85, p102, p104, p108, p110-112, p116, p118-119, p123-126, p128-p136, p138-139, p142-144, p171, p180, p183.||Seaspray Group||Overlain by the Gippsland Limestone.|Marls.|
10081|Lakes Entrance Formation|67061|6|Mentioned|p554 Fig.10.|Miocene||Gippsland Basin, onshore.||Unit in Seaspray Group.||Is overlain by Gippsland Formation.||
10081|Lakes Entrance Formation|67727|5|Briefly described|p55, p58 Fig.2, p62, p78.|Oligocene|Oligocene|Gippsland Basin, mainly offshore. Equivalent to the Morwell Formation in the Latrobe Valley.||Unit in Seaspray Group.|Includes Giffard Sandstone.|Overlies Traralgon Formation. Is overlain by Haunted Hill Formation.|Marls and limestones.|
10081|Lakes Entrance Formation|69016|5|Briefly described|p88-89|||Of the Gippsland Basin.||Unit of Seaspray Group.||Laterally grades into lower unit of Balook Formation.|Sands and gravels at the base, developing to finer grained marls and mudstone on the top with fine interbeds of fossiliferous sandy limestone.|
10081|Lakes Entrance Formation|70028|5|Briefly described|p77-82, 86, 88-91|Oligocene|Oligocene|Gippsland Basin. Regional seal to the Latrobe Group reservoirs. Rated as excellent to good for CO2 storage.||Basal Seaspray Group.||Is overlain by the Gippsland Limestone.|Fine-grained sediments: mainly marl and rich in smectite clay.|
10081|Lakes Entrance Formation|70076|5|Briefly described|South-Eastern:p2. Regional: Fig.3; p3,p6|Burdigalian|Rupelian|Onlapping, marly sediments provide the principal regional seal across the Basin.||Basal unit in Seaspray Group.|Seacombe Marl, and Giffard Sandstone, Members.|Overlies Gurnard or Burong Formation. Is overlain by Gippsland Limestone.||
10081|Lakes Entrance Formation|70862|6|Mentioned|p48 Fig.1|||Latrobe Valley, Gippsland Basin.||Seaspray Group.||Overlies Traralgon Formation. Is overlain by Gippsland Limestone Formation.||
10081|Lakes Entrance Formation|73289|5|Briefly described|p765 Fig.2, 767, 770, 773-774|Oligocene|Oligocene|Lake Wellington, Seaspray Depressions, onshore Gippsland Basin.||Seaspray Group.|Giffard Sandstone Member.|Overlies Traralgon Formation. Is overlain by Gippsland Limestone Formation. Interfingers with (lateral facies variation of) Balook Formation.||
10081|Lakes Entrance Formation|73471|5|Briefly described|p86-87, p89|||Gippsland Basin. Overlies Latrobe Unconformity. Acts as the regional seal to oil and gas. See also Lakes Entrance Subgroup.||Seaspray Group||Overlies Gurnard Formation|Marls and marine carbonates.|
10081|Lakes Entrance Formation|73488|4|Described|p631-632, p634 Fig.4, p636-637, p646|Chattian|Rupelin|Gippsland Basin.||Seaspray Group||Overlies Giffard Sandstone, underlies Gippsland Limestone Formation|Marine carbonate sediments. Marls and glauconitic mudstones.|
10081|Lakes Entrance Formation|73562|5|Briefly described|p303-304|Miocene|Oligocene|Gippsland Basin; offshore. Has extensive submarine canyoning.||Basal Seaspray Group.||Equivalent to (lower part of) the Balook Formation.|Marine mudstone and limestone.|
10081|Lakes Entrance Formation|75065|5|Briefly described|p151-152, 154, 170-171|Pliocene|Eocene|Gippsland Basin; offshore.||Seaspray Group.||Overlies Gurnard Formation locally. Is overlain by Gippsland Limestone.|Deep-water marls.|
10170|Langra Formation|22562|6|Mentioned|p39|||||||||
10170|Langra Formation|22760|5|Briefly described|p340|||Of the Finke Group.||||||13-OCT-06
10170|Langra Formation|22826|4|Described|p576|Devonian|Devonian|Of the Finke Group.||||||13-OCT-06
10170|Langra Formation|24301|5|Briefly described|p22|||Geological Province: Amadeus Basin||||||
10170|Langra Formation|30544|6|Mentioned|Fig.5 P51|||Map legend||||||
10170|Langra Formation|31566|6|Mentioned|p244|||Devonian||||||
10170|Langra Formation|31567|3|Fully described|p280|||Refers Wells et al. (1966).||||||
10170|Langra Formation|33971|3|Fully described|p30|||Refers Wells et al. (1966).||||||
10170|Langra Formation|34111|5|Briefly described|Table 2|||See also pp16-19. Devonian - Carboniferous.||||||13-OCT-06
10170|Langra Formation|34580|4|Described|Table 1|||Devonian - Carboniferous||||||
10170|Langra Formation|35102|6|Mentioned|Fig.17|||||||||
10170|Langra Formation|42699|5|Briefly described|map legend|Devonian||||||||
10170|Langra Formation|42940|6|Mentioned|Plate 5|||||||||
10170|Langra Formation|43035|5|Briefly described|p24|||Of Finke Group.||||||13-OCT-06
10170|Langra Formation|44133|5|Briefly described|p44|Carboniferous?|Late Devonian|Of the Finke Group. Conformably overlies Mereenie Sandstone. Overlain by Horseshoe Bend Shale.||||||
10170|Langra Formation|44323|14|Not recorded|map legend|Carboniferous|Devonian|SG/53-6, Dev-Carb pt of Finke Group.||||||
10170|Langra Formation|44393|4|Described|p.3,7,8,Tb.1,Fig.1|Carboniferous|Devonian|Part of Finke Group. Dev-Carb.||||||
10170|Langra Formation|44433|14|Not recorded|map legend|||Devonian to Carboniferous.||||||
10170|Langra Formation|45041|4|Described|p104|||Devonian||||||
10170|Langra Formation|48865|2|Defined|p.4,10,Fig.29|Carboniferous|Devonian|On many figures. Fig.4,11,21,28,36,39,51,53,55,Pl.3,4,5,11. Unit of Finke Gp.Devn-Carb. (G53-6)||||||
10170|Langra Formation|48890|4|Described|p.51|Carboniferous|Devonian|See also, Tb.2,Tb.3,Fig.4. p.52, Pl.9. pt. Finke Gp. Dev-Carb.||||||
10170|Langra Formation|50372|5|Briefly described|Map Legend|Devonian|Devonian|Of Finke Group. Geological Province: Amadeus Basin. Weathered fine to medium grained crossbedded quartz sandstone with rare conglomeritic lenses with basement clasts.||||||
10170|Langra Formation|65233|5|Briefly described|p13|||Interfingers with pertnjara Group.||||||07-FEB-11
10170|Langra Formation|65309|4|Described|p6 Table 1, pp13-14, pp19-20.|Devonian|Devonian|Most exposures thin and consist of upper part of sequence. Drilling shows thickness ranges from 0 to 130m. Includes angular clasts of Stairway Sandstone. Type area at Polly Corner.||Unit in Finke Group.||Partly overlies, and partly a distal equivalent of, Polly Conglomerate.|Very weathered, fine to medium, cross-bedded quartz sandstone; rare conglomeratic lenses with basement clasts; red and blue clayey shale encountered in drillholes.|
10170|Langra Formation|65489|6|Mentioned|p63|||Amadeus Basin. Contains potential reservoir beds. The middle unit could act as a seal.||||||
10170|Langra Formation|69438|4|Described|p23:2-3, 10, 20, 40-41|Late Devonian|Late Devonian|Wells et al. (1966). Amadeus Basin. Up to 527m thick. Becomes finer-grained northwards and up-section. Fluvial: mainly point-bar deposits.||Finke Group.||Conformably/gradationally overlies Polly Conglomerate. Unconformably overlies Larapinta Group, Parke Siltstone, Winnall beds, Bitter Springs Formation. Is overlain conformably by Horseshoe Bend Shale.|Cycles of massive conglomerate beds overlain by sandstone and an upper sandy siltstone, overlain by pebbly cross-bedded sandstone; then sandy micaceous siltstone; topped by fine- to medium-grained sandstone succession with few pebbly intervals.|12-JUL-16
10170|Langra Formation|69449|5|Briefly described|p34:5|Devonian|Devonian|||Finke Group.||Overlies Polly Conglomerate. Is overlain by Horseshoe Bend Shale.|Massive sandstone with minor claystone.|12-JUL-16
10170|Langra Formation|69673|6|Mentioned|p64 fig 53, p149|||||Finke Group||Overlies Polly Conglomerate, overlain by Horseshoe Bend Shale, Idracowra Sandstone||
10170|Langra Formation|71279|5|Briefly described|p355 Fig.2|Late Devonian|Late Devonian|Amadeus Basin.||Finke Group.||||
10170|Langra Formation|73085|6|Mentioned|p1|late Devonian|late Devonian|||Finke Group||Underlain by Polly Conglomerate. Overlain by Horseshoe Bend Shale / Idracowra Sandstone. Equivalent to Hermannsburg Sandstone (Pertnjara Group).||
10170|Langra Formation|73281|6|Mentioned|Appendix (DIP)|||See DIP034_Petroleumdata.xlsx and DIP034_Welldata.xlsx.||||||
10172|Langwarren Formation|29780|6|Mentioned|p50|||||||||
10172|Langwarren Formation|43052|5|Briefly described|Table 2.1|||||||||
10172|Langwarren Formation|44133|5|Briefly described|p198, 153 Fig. 10.2|Late Eocene|Middle Eocene|Geological Province: Hamilton Basin.||||||
10172|Langwarren Formation|67462|5|Briefly described|Map legend.|Early Oligocene|Middle Eocene|Willochra Basin.||||||
10172|Langwarren Formation|68715|6|Mentioned|p31 Fig.5|Eocene|Eocene|Willochra Basin. Late Eocene age.||||||
10184|Larapinta Group|9199|5|Briefly described|Map legend|Ordovician|Cambrian|Includes the Pacoota Sandstone.  Geological Province: Amadeus Basin.||||||
10184|Larapinta Group|9814|5|Briefly described|Map Legend|Ordovician|Ordovician|||||||
10184|Larapinta Group|13995|5|Briefly described|p69|Ordovician|Ordovician|Amadeus Basin.|||Stairway Sandstone.|||
10184|Larapinta Group|22561|6|Mentioned|p11|||||||||
10184|Larapinta Group|22563|6|Mentioned|p47||Ordovician|||||||
10184|Larapinta Group|22566|5|Briefly described|p76|Devonian|Late Cambrian|||||||
10184|Larapinta Group|22650|6|Mentioned|Fig 2 on p 157|Ordovician|Cambrian|||||||
10184|Larapinta Group|22651|6|Mentioned|p 189|||||||||
10184|Larapinta Group|22655|6|Mentioned|p 255|||informally divided in to upper and lower Larapinta Group, p255.||||||17-JAN-07
10184|Larapinta Group|22656|6|Mentioned|Fig 4 on p 282|Ordovician|Cambrian|||||||
10184|Larapinta Group|22760|5|Briefly described|p339|||||||||
10184|Larapinta Group|22761|6|Mentioned|Fig 2 on p351|Ordovician||||||||
10184|Larapinta Group|22763|6|Mentioned|p394|Late Ordovician|Cambrian|||||||
10184|Larapinta Group|22804|4|Described|p451|Early Devonian|Late Cambrian|||||||
10184|Larapinta Group|22805|6|Mentioned|p471|||||||||
10184|Larapinta Group|22806|6|Mentioned|p485||Ordovician|||||||
10184|Larapinta Group|22807|6|Mentioned|Fig 3 on p495|Late Ordovician|Early Ordovician|||||||
10184|Larapinta Group|22824|5|Briefly described|p525|Ordovician|Cambrian|||||||
10184|Larapinta Group|22826|6|Mentioned|Fig 4 on p567|||||||||
10184|Larapinta Group|23858|6|Mentioned|p914|||Geological Province: Amadeus Basin.||||||
10184|Larapinta Group|24063|5|Briefly described|p220|Ordovician|Cambrian|Geological Province: Amadeus Basin.||||||
10184|Larapinta Group|24064|5|Briefly described|p229 Fig.7|Ordovician|Ordovician|Geological Province: Amadeus Basin.||||||
10184|Larapinta Group|24111|6|Mentioned|p214 Fig. 9|||Geological Province: Amadeus Basin.||||||24-MAR-05
10184|Larapinta Group|24301|5|Briefly described|p20|Ordovician|Ordovician|Includes Stairway Sandstone, Stokes Siltstone and Carmichael Sandstone.   Geological Province: Amadeus Basin||||||
10184|Larapinta Group|24302|5|Briefly described|Map Legend|Ordovician|Ordovician|Includes the Stairway Sandstone, Stokes Siltstone and Carmichael Sandstone. Geological Province: Amadeus Basin.||||||16-JUL-13
10184|Larapinta Group|29721|6|Mentioned|Table 44|||||||||
10184|Larapinta Group|29972|6|Mentioned|p4|||Upper Cambrian- Ordovician||||||
10184|Larapinta Group|30238|4|Described|p64|||Cambrian - Ordovician age.||||||17-JAN-07
10184|Larapinta Group|30258|6|Mentioned|Fig.2|||Ordovician age||||||
10184|Larapinta Group|30544|6|Mentioned|p49|||||||||
10184|Larapinta Group|30817|6|Mentioned|p14|||||||||
10184|Larapinta Group|31566|6|Mentioned|p230|||Ordovician||||||
10184|Larapinta Group|31567|6|Mentioned|p280|||Unconformably overlain by Langra Formation.||||||17-JAN-07
10184|Larapinta Group|31707|4|Described|p50|||Discussed.||||||17-JAN-07
10184|Larapinta Group|32208|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
10184|Larapinta Group|32209|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
10184|Larapinta Group|33192|6|Mentioned|p20|||||||||
10184|Larapinta Group|33307|6|Mentioned|Fig.6|||||||||
10184|Larapinta Group|33738|6|Mentioned|p52|||||||||
10184|Larapinta Group|33761|6|Mentioned|p146|||Ord.- Sil? - Dev.||||||
10184|Larapinta Group|33971|5|Briefly described|p28|||Strat. section Fig.15.||||||
10184|Larapinta Group|34111|5|Briefly described|Table 2|||Cambrian - Ordovician. See also pp15-18.||||||13-OCT-06
10184|Larapinta Group|34186|6|Mentioned|Fig.4|||Ordovician||||||
10184|Larapinta Group|34442|5|Briefly described|Table 1|||Cambrian - Ordovician. See also pp8,9,10,11.||||||13-OCT-06
10184|Larapinta Group|34488|6|Mentioned|p11|||||||||
10184|Larapinta Group|34579|4|Described|Table 2|||Cambrian - Ordovician. See pp10,15,16.||||||13-OCT-06
10184|Larapinta Group|34580|4|Described|Table 1|||Ordovician||||||
10184|Larapinta Group|35102|6|Mentioned|p4|||||||||
10184|Larapinta Group|36198|6|Mentioned|Fig.III.2|||||||||
10184|Larapinta Group|36473|6|Mentioned|Map legend|Ordovician|Adelaidean|Adelaidean to Ordovician||||||
10184|Larapinta Group|36643|6|Mentioned|p65|||||||||
10184|Larapinta Group|36818|6|Mentioned|p203|||||||||
10184|Larapinta Group|36821|6|Mentioned|p397|||||||||
10184|Larapinta Group|38329|6|Mentioned|p210|||||||||
10184|Larapinta Group|38606|6|Mentioned|Map legend|Early Ordovician|Late Cambrian|Late Cambrian to Early Ordovician||||||
10184|Larapinta Group|38885|6|Mentioned|Map legend|Early Ordovician|Late Cambrian|Late Cambrian - Early Ordovician||||||
10184|Larapinta Group|39565|6|Mentioned|p33|||||||||
10184|Larapinta Group|39583|6|Mentioned|Map legend|Early Ordovician|Late Cambrian|Late Cambrian to Early Ordovician||||||
10184|Larapinta Group|39931|6|Mentioned|Map legend|Early Ordovician|Late Cambrian|Late Cambrian to Early Ordovician||||||
10184|Larapinta Group|40136|5|Briefly described|p29|||||||||
10184|Larapinta Group|40201|5|Briefly described|Table 1|||||||||
10184|Larapinta Group|40740|3|Fully described|p46|||Mention p6.||||||13-OCT-06
10184|Larapinta Group|40810|4|Described|p7|||||||||
10184|Larapinta Group|41018|6|Mentioned|p236|||||||||
10184|Larapinta Group|41039|6|Mentioned|Fig.2|||||||||
10184|Larapinta Group|41115|6|Mentioned|p1400|||||||||
10184|Larapinta Group|41190|6|Mentioned|p267|||||||||
10184|Larapinta Group|41203|5|Briefly described|p4|||||||||
10184|Larapinta Group|41224|5|Briefly described|p430|||||||||
10184|Larapinta Group|41270|6|Mentioned|p272|||||||||
10184|Larapinta Group|41385|6|Mentioned|Fig.3|||||||||
10184|Larapinta Group|41621|5|Briefly described|Map legend|Late Ordovician|Late Cambrian|||||||
10184|Larapinta Group|41711|6|Mentioned|p259|||||||||
10184|Larapinta Group|41717|6|Mentioned|Fig.2|||||||||
10184|Larapinta Group|41723|6|Mentioned|Map legend|Ordovician||||||||
10184|Larapinta Group|41801|5|Briefly described|p212|||||||||
10184|Larapinta Group|41819|6|Mentioned|Map legend|Late Ordovician|Late Cambrian|||||||
10184|Larapinta Group|41820|5|Briefly described|p7|||||||||
10184|Larapinta Group|42060|6|Mentioned|Fig.5 P140|||||||||
10184|Larapinta Group|42082|6|Mentioned|p322|||||||||
10184|Larapinta Group|42141|6|Mentioned|Fig.3 P570|||||||||
10184|Larapinta Group|42354|5|Briefly described|p3, p6|||Defined by Prichard and Quinlan (1962).||||||17-JAN-07
10184|Larapinta Group|42504|6|Mentioned|p77|||||||||
10184|Larapinta Group|42699|5|Briefly described|map legend|Ordovician||||||||
10184|Larapinta Group|42940|5|Briefly described|Plate 2|Ordovician|Ordovician|Siltstone, sandstone, limestone, dolostone, phosphorite; marine fossils.  Age: 500-440Ma. Geological province: Amadeus Basin.||||||23-JAN-08
10184|Larapinta Group|43035|5|Briefly described|p21|||||||||
10184|Larapinta Group|43105|5|Briefly described|Fig.3,p8.|||||||||
10184|Larapinta Group|43225|5|Briefly described|Map Legend||Ordovician|In the Amadeus Basin.||||||17-JAN-07
10184|Larapinta Group|43503|6|Mentioned|32-50|Silurian|Late Cambrian|||||||
10184|Larapinta Group|43631|6|Mentioned|p26|||||||||
10184|Larapinta Group|43647|6|Mentioned|Fig.4,533|||||||||
10184|Larapinta Group|43648|5|Briefly described|Fig.1,p488|||||||||
10184|Larapinta Group|43649|5|Briefly described|fig.1,p454-455,459|||||||||
10184|Larapinta Group|43817|6|Mentioned|Fig.1,p42|||||||||
10184|Larapinta Group|44133|5|Briefly described|p43|||Includes: Stairway Sandstone.||||||
10184|Larapinta Group|44323|14|Not recorded|map legend||Ordovician|SG/53-6. Ordovician.||||||
10184|Larapinta Group|44342|4|Described|p.6, Table 2||Ordovician|SG/53-5. U-M Ordovician.||||||
10184|Larapinta Group|44343|14|Not recorded|map legend||Late Ordovician|U.Ordovician.||||||
10184|Larapinta Group|44393|6|Mentioned|p.7|||refs Wells et al 1968.||||||
10184|Larapinta Group|44395|14|Not recorded|p.8,9,12,13, Tb.2|||||||||
10184|Larapinta Group|44402|5|Briefly described|map legend|Ordovician|Cambrian|Includes Stokes Siltstone, Stairway Sandstone, Horn Valley Siltstone, Pacoota Sandstone. Camb-Ord.||||||02-DEC-04
10184|Larapinta Group|44433|14|Not recorded|map legend|||Cambrian to Ordovician.||||||
10184|Larapinta Group|44484|14|Not recorded|p.3,5,10,Fig.4,Tb.1|Ordovician|Cambrian|Camb-Ord. See also p.12,14, for more details.||||||
10184|Larapinta Group|44485|14|Not recorded|map legend|Ordovician|Cambrian|Includes Pacoota Sandstone, Horn Valley Siltstone, Stairway Sandstone, Carmichael Sandstone, Stokes Siltstone. Camb-Ord.||||||
10184|Larapinta Group|44493|4|Described|p.11||Ordovician|BLOODS RANGE sheet (G53-3). See p.8,13, for details.||||||22-DEC-09
10184|Larapinta Group|44494|14|Not recorded|map legend||Ordovician|||||||
10184|Larapinta Group|44497|4|Described|p.10-11, Table 2|Ordovician|Cambrian|SF/53-13. Cambrian-Ord.||||||
10184|Larapinta Group|44498|14|Not recorded|map legend|Ordovician|Cambrian|Camb-Ord.||||||
10184|Larapinta Group|44505|14|Not recorded|p.2,7,8,10,11, Fig 1|Ordovician|Cambrian|Camb-Ord.||||||
10184|Larapinta Group|44506|14|Not recorded|map legend|Ordovician|Cambrian|Cambrian-Ordovician.||||||
10184|Larapinta Group|45036|6|Mentioned|p3|||Upper Cambrian - Upper Ordovician age||||||
10184|Larapinta Group|45041|4|Described|p61|||See also pp62-86. Ordovician.||||||13-OCT-06
10184|Larapinta Group|45118|6|Mentioned|p3|||||||||
10184|Larapinta Group|45155|6|Mentioned|p36|||See also Fig.37||||||
10184|Larapinta Group|45170|6|Mentioned|Fig.8|||||||||
10184|Larapinta Group|46829|6|Mentioned|Fig.2|||||||||
10184|Larapinta Group|46856|6|Mentioned|p279|||||||||
10184|Larapinta Group|46928|6|Mentioned|Table 1|||||||||
10184|Larapinta Group|47050|6|Mentioned|Fig.2|||||||||
10184|Larapinta Group|47052|6|Mentioned|p261|||||||||
10184|Larapinta Group|48639|14|Not recorded|p.16,opp.p.1|Ordovician|Cambrian|Ord-Cam. (G55-2).||||||
10184|Larapinta Group|48838|2|Defined|p.18,22, Tb.1,2|||||||||
10184|Larapinta Group|48862|14|Not recorded|p.1,18,24-29,39-42|||(F52-15). Pl.10,11.||||||
10184|Larapinta Group|48863|14|Not recorded|p.30||Ordovician|Tb.1. opp.p.7,p.2,7,12,24,30,31,37,39-42,Pl.11,13,15,16. (G52-4,G53-1).||||||
10184|Larapinta Group|48864|2|Defined|p.32||Ordovician|Tb.1. On many pages. p.2,9,10,27,38,30,34,37,47,50,Pl.11. (G52-3). Ord.||||||
10184|Larapinta Group|48865|4|Described|p.23||Ordovician|Includes: Pacoota Sandstone, Horn Valley Fm, Stokes Fm, Stairway Sandstone. Ord. On many pages. p.20,21,27,45-47,50,Pl.8.||||||
10184|Larapinta Group|48880|14|Not recorded|p.20,33,Pl.10,11||Ordovician|(F53-13,F53-14). Ord.||||||
10184|Larapinta Group|48890|4|Described|p.44-47|Ordovician|Cambrian|See also Tables, Figs and Plates. Camb-Ord.||||||13-OCT-06
10184|Larapinta Group|48963|6|Mentioned|p2|||p22||||||13-OCT-06
10184|Larapinta Group|50098|5|Briefly described|p1|Ordovician|Late Cambrian|Includes the Pacoota Sandstone, Horn Valley Siltstone, Stairway Sandstone, Stokes Siltstone and Carmichael Sandstone. Geological Province: Amadeus Basin.||||||
10184|Larapinta Group|50286|5|Briefly described|Map Legend|Ordovician|Ordovician|Geological Province: Amadeus Basin.||||||
10184|Larapinta Group|60547|5|Briefly described|Map Legend|Ordovician|Cambrian|Geological Province: Amadeus Basin.||||||
10184|Larapinta Group|60572|5|Briefly described|Map legend|Ordovician|Ordovician|White sandstone, locally bioturbated, minor siltstone, and conglomeratic sandstone.  Geological Province: Amadeus Basin.||||||23-DEC-09
10184|Larapinta Group|60674|5|Briefly described|Map legend|Ordovician|Cambrian|Includes: Pacoota Sandstone, Horn Valley and Stokes Siltstones, and Carmicahel Sandstone.  Geological Province: Amadeus Basin.||||||27-MAY-09
10184|Larapinta Group|60678|5|Briefly described|Map legend|Ordovician|Ordovician|White sandstone, locally bioturbated; minor siltstone and conglomeratic sandstone.  Geological Province: Amadeus Basin.||||||
10184|Larapinta Group|60679|5|Briefly described|Map Legend|Ordovician|Ordovician|Sandstone, minor siltstone and conglomeratic sandstone. Geological Province: Amadeus Basin.||||||
10184|Larapinta Group|60683|4|Described|p26, p9 Tb. 1|Ordovician|Ordovician|White sandstone, locally bioturbated, with minor siltstone and conglomeratic sandstone. Geological Province: Musgave Block/ Amadeus Basin.||||||16-JUN-09
10184|Larapinta Group|60904|5|Briefly described|p790 Fig. 16|Middle Ordovician|Late Cambrian|Marine sediments.||||||
10184|Larapinta Group|61386|5|Briefly described|Map legend|Cambrian|Cambrian|White sandstone, locally bioturbated, minor siltstone and conglomeratic sandstone. Geological Province: Amadeus Basin.||||||23-DEC-09
10184|Larapinta Group|61387|5|Briefly described|Map legend|Ordovician|Ordovician|Includes the Pacoota Sandstone, Horn Valley Siltstone, Stairway and Carmichael Sandstones. Geological Province: Amadeus Basin.||||||17-JAN-07
10184|Larapinta Group|61518|5|Briefly described|Map Legend|Ordovician|Cambrian|Geological Province: Amadeus Basin.||||||
10184|Larapinta Group|61519|5|Briefly described|Map Legend|Ordovician|Ordovician|Geological Province: Amadeus Basin.||||||
10184|Larapinta Group|62376|5|Briefly described|p18|Early Devonian|Late Cambrian|Geological Province: Amadeus Basin.||||||09-FEB-10
10184|Larapinta Group|62379|5|Briefly described|p7 Fig. 2|Devonian|Late Cambrian|Geological Province: Amadeus Basin.||||||
10184|Larapinta Group|62609|5|Briefly described|Map Legend|Ordovician|Cambrian|Siltstone, sandstone, limestone, dolomite, phosphorite. Underlies: Mereenie Sandstone. Overlies: Pertaoorrta Group.||||||14-AUG-06
10184|Larapinta Group|62620|5|Briefly described|Map Legend|Ordovician|Cambrian|Siltstone, sandstone, limestone, dolomite, phosphorite.||||||
10184|Larapinta Group|62794|5|Briefly described|p288, p289 Fig.2, p290|Ordovician|Late Cambrian|In Amadeus Basin, southern Northern Territory. Over 2100 m thick. Comprises (in ascending order) Pacoota Sandstone, Horn Valley Siltstone, Stairway Sandstone, Stokes Siltstone, Carmichael Sandstone.||||||
10184|Larapinta Group|62982|5|Briefly described|p7|Late Ordovician|Late Cambrian|Includes the Pacoota Sandstone at its base. Thick marine deposits. Geological Province: Amadeus Basin. Hosts two producing oil and gas fields.||||||16-JAN-07
10184|Larapinta Group|63562|6|Mentioned|p348-349|Middle Ordovician|Late Cambrian|Of Amadeus Basin.|||Includes Pacoota and Stairway Sandstones, and Horn Valley and Stokes Siltstones.|||
10184|Larapinta Group|64334|5|Briefly described|p37, 40, 42, 45, 47|Ordovician|Late Cambrian|Prichard and Quinlan (1962). Originally the Larapintine Series of Tate (1896), using the Aboriginal name for the Finke River. Mostly shallow-marine. Up to 2300m thick.|||Pacoota, Carmichael Sandstones; Horn Valley, Stairway, Stokes Siltstones.|Unconformably overlies Pertaoorrta Group.||
10184|Larapinta Group|64778|6|Mentioned|p12-13|Ordovician|Ordovician|Amadeus Basin. Post-Delamerian Orogeny sediments; thickening to N; over 2000m.||||||
10184|Larapinta Group|64809|6|Mentioned|p3 Fig.2, p6 Fig.4 |Early Devonian|Proterozoic||||Includes the Stairway Sandstone, Horn Valley Siltstone and Pacoota Sandstone.|||
10184|Larapinta Group|64970|6|Mentioned|p719 Fig. 2|Silurian|Ordovician|Geological Province: Amadeus Basin.||||||27-MAY-09
10184|Larapinta Group|65102|6|Mentioned|p363, Figure 4-38|Paleozoic|Paleozoic|Amadeus Basin.||||||
10184|Larapinta Group|65233|3|Fully described|p3 Fig. 2, p9|Silurian|Late Cambrian|Informally divided into Lower - Upper Larapinta Groups; upper comprises Carmichael and Mereenie Sandstones; lower consists of Pacoota and Stairway Sandstone, and Horn Valley and Stokes Siltstones. Unconformably overlies Goyder Formation. In Amadeus Basin.||||||16-JUL-13
10184|Larapinta Group|65256|5|Briefly described|p6 Tb.1, p24, p16, p19|Ordovician|Ordovician|White to red sandstone, locally bioturbated, minor siltstone, conglomeratic sandstone and limestone interbeds; fossiliferous. Onlaps Dean Quartzite; unconformably overlies Pottoyu Granite Suite; may directly overlie basement; locally overlies Winnall beds. Some sections contain angular clasts of Dean Quartzite. Includes Stokes Siltstone. >10m thick.||||||
10184|Larapinta Group|65272|6|Mentioned|p319, p320 Fig.3|Ordovician|Cambrian|Northern Amadeus Basin. Thick marine sequences coeval with the Larapinta Event.||||||
10184|Larapinta Group|65489|5|Briefly described|p125|Ordovician|Cambrian|Amadeus Basin.|||Includes Pacoota, Stairway and Carmichael Sandstones; Horn Valley and Stokes Siltstones.|Overlies Pertaoorrta Group.||
10184|Larapinta Group|66767|5|Briefly described|p60|Ordovician|Ordovician|NE Amadeus Basin.|||Horn Valley Siltstone.|Overlies Pertaoorta Group. Is overlain by Mereenie Sandstone.|Predominantly siliciclastic sedimentary rocks.|
10184|Larapinta Group|67326|5|Briefly described|p2-3|Early Devonian|Late Cambrian|Amadeus Basin.|||Pacoota, Stairway, Carmichael, Mereenie Sandstones; Horn Valley, Stokes Siltstones.|Overlies Pertaoorrta Group. Is overlain by Pertnjara Group.||
10184|Larapinta Group|67565|5|Briefly described|p5 Fig.3, pp41-42.|||Amadeus Basin.|||Includes Pacoota Sandstone, Horn Valley Siltstone, Stairway Sandstone, Stokes Siltstone, Carmichael Sandstone.|||03-DEC-15
10184|Larapinta Group|67856|5|Briefly described|p338 fig 4-30|Late Ordovician|Late Cambrian||||Includes Pacoota Sandstone, Horn Valley Siltstone, Stairway Sandstone, Stokes Siltstone, Carmichael Sandstone.|||
10184|Larapinta Group|68316|6|Mentioned|p779, p785|Ordovician|Ordovician|Amadeus Basin.||||||
10184|Larapinta Group|68323|6|Mentioned|p4 Fig.2|Early Devonian|Late Cambrian|Amadeus Basin.|||Pacoota, Stairway, Carmichael, Mereenie Sandstones; Horn Valley, Stokes Siltstones.|||
10184|Larapinta Group|69438|5|Briefly described|p23:2-5, 7-8, 20, 32-39, 46, 50, 60|Late Ordovician|Late Cambrian|Defined, as were its constituent Formations, by Pritchard and Quinlan (1962); after the Larapintine Series of Tate (1896). They included sandstone of the Carmichael Sandstone in the upper Stokes Siltstone (others mapped it as lower Mereenie Sandstone). Amadeus Basin.|||Pacoota, Stairway, Carmichael Sandstones; Horn Valley, Stokes Siltstones.|Is overlain disconformably by Dare Siltstone Member (Parke Siltstone).||12-JUL-16
10184|Larapinta Group|69444|6|Mentioned|p29:6|Ordovician|Ordovician|Amadeus Basin. Deposition was coincident with tectonism (the Larapinta Event) with peaks at 475 Ma and 460 Ma.||||||12-JUL-16
10184|Larapinta Group|69449|5|Briefly described|p34:4|Ordovician|Ordovician|Amadeus Basin.|||Pacoota Sandstone.|||12-JUL-16
10184|Larapinta Group|69458|6|Mentioned|p42:8|Ordovician|Ordovician|Amadeus Basin.||||||12-JUL-16
10184|Larapinta Group|69606|5|Briefly described|p4 fig 2|Ordovician|Cambrian|Misspelling of the Larapinta Group. Amadeus Basin. The carbonate shales and muds are potential source and seal rocks whilst the sandstones are potential reservoir rocks.||||Unconformably overlies the Upper Pertaoorta Group. Overlain by the Carmichael Sandstone.|Interbedded sandstone, carbonate, shale and marl.|
10184|Larapinta Group|69673|6|Mentioned|p66, p102, p103||||||Includes Pacoota Sandstone, Horn Valley Siltstone, Stairway Sandstone, Stokes Siltstone, Carmichael Sandstone|||
10184|Larapinta Group|70749|6|Mentioned|p54|||Amadeus Basin.|||Pacoota Sandstone.|||
10184|Larapinta Group|71146|5|Briefly described|p6|Wenlock|Cambrian|Amadeus Basin.|||Includes the Pacoota Sandstone, Horn Valley Siltstone, Stairway Sandstone, Stokes Siltstone and the Carmichael Sandstone.|Unconformably overlies the Pertaoorrta Group.|Sandstone, carbonate, mudstone and coal.|
10184|Larapinta Group|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||siltstone, sandstone|
10184|Larapinta Group|71268|5|Briefly described|1m_geologyp12_lut.csv||||||||Marine sediments. White sandstone, locally bioturbated; minor siltstone and conglomeratic sandstone.|
10184|Larapinta Group|71279|5|Briefly described|p355 Fig.2, p363, p365, p374, p382 Tb.1|Early Devonian|Late Cambrian|Amadeus Basin. Modelled magnetic properties.|||Pacoota, Stairway, Carmichael, Mereenie Sandstones; Horn Valley, Stokes Siltstones.|||
10184|Larapinta Group|71898|5|Briefly described|iii, p1, p3, p17, p20-p22|||Amadeus Basin. Outcrops on the PALM VALLEY Sheet (5440) of the HENBURY Sheet (SG 53-01).|||Includes the Horn Valley Siltstone and the Pacoota Sandstone.|Overlies the Pertaoorrta Group.||19-NOV-18
10184|Larapinta Group|71965|6|Mentioned|p911|||Of Amadeus Basin.||||Correlable to Warratta Group.||
10184|Larapinta Group|72360|5|Briefly described|Map legend|Ordovician|Cambrian|Of Amadeus Basin.|||Includes Carmichael Sandstone, Stairway Sandstone, Horn Valley Siltstone and Pacoota Sandstone.|||09-SEP-19
10184|Larapinta Group|72369|5|Briefly described|iii,26,37|Devonian|Ordovician|Of Amadeus Basin.|||Includes Pacoota and Stairway sandstones, Stokes Siltstone, and the Carmichael and Mereenie sandstones, Parke Siltstone, Horn Valley Siltstone.|||
10184|Larapinta Group|72374|5|Briefly described|iii,p3,17|||Of Amadeus Basin.|||Layout implies includes Carmichael and Mereenie sandstones.|||11-OCT-19
10184|Larapinta Group|72476|6|Mentioned|p36 Fig.9|||Amadeus Basin. Time-temperature thermal history diagram.||||||
10184|Larapinta Group|73085|6|Mentioned|p1, p4|early Devonian|late Cambrian||||Mereenie Sandstone, Carmichael Sandstone, Stokes Siltstone, Stairway Sandstone, Horn Valley Siltstone, Pacoota Sandstone.|||
10184|Larapinta Group|73119|6|Mentioned|piii, p19|||Amadeus Basin, western.|||Stairway Sandstone|||
10184|Larapinta Group|73279|6|Mentioned|p10-14|Ordovician|Cambrian|Amadeus Basin.|||Pacoota Sandstone, Stairway Sandstone, Stokes Siltstone, Carmichael Sandstone|||
10184|Larapinta Group|73437|6|Mentioned|p152|||Apatite fission track cooling age of 341+/-58 Ma from Tingate, (1990).||||||
10273|Le Hunte Formation|30756|2|Defined|p2|Holocene|Holocene|||||||
10273|Le Hunte Formation|30922|6|Mentioned|Map legend|Holocene|Holocene|||||||
10273|Le Hunte Formation|35772|4|Described|Table 1|||||||||
10273|Le Hunte Formation|42466|6|Mentioned|Map Legend|||||||||
10273|Le Hunte Formation|42475|6|Mentioned|p26|||of Firman 1974.||||||
10273|Le Hunte Formation|44133|5|Briefly described|p220 Fig. 11.2, 236|Holocene|Pleistocene|same as Le Hunt Formation?? Of the Saint Kilda Formation.||||||
10273|Le Hunte Formation|44864|5|Briefly described|Map Legend||Holocene|||||||
10273|Le Hunte Formation|61155|5|Briefly described|p17|Holocene|Late Pliocene|Age: <2Ma. Geological Province: Eucla Basin.||||||
10286|Leasingham Quartzite Member|22889|4|Described|p37 & p39|Adelaidean|Adelaidean|See p39 for location of type section and description of unit. The Leasingham Quartzite Member superseds the former Leasingham Quartzite as the unit has been down graded from formation to member status, see p37 for details of change.||||||
10286|Leasingham Quartzite Member|41404|5|Briefly described|p114|||||||||
10286|Leasingham Quartzite Member|42222|6|Mentioned|p14|||||||||
10286|Leasingham Quartzite Member|43052|5|Briefly described|p181,Table 6.1|||Of Auburn Dolomite.||||||30-SEP-08
10286|Leasingham Quartzite Member|61732|5|Briefly described|p28 Fig. 13|Sturtian|Sturtian|Of the Mintaro Shale (Belair Subgroup, Umberatana Group). Geological Province: Adelaide Rift Complex.||||||07-FEB-11
10317|Leigh Creek Coal Measures|13516|6|Mentioned|p164|Late Triassic|Late Triassic|From SA.||||||
10317|Leigh Creek Coal Measures|23818|5|Briefly described|p135 Fig.61, p136|Rhaetian|Early Triassic|Max. thickness: 2000 ft.||||||
10317|Leigh Creek Coal Measures|24138|5|Briefly described|p10 Fig. 1.1|Triassic|Triassic|||||||
10317|Leigh Creek Coal Measures|24176|3|Fully described|p18, p22 Tb. 1|Triassic|Triassic|Grey siltstones, minor sandstones carbonaceous shales, ferruginous siltstones, coal seams, basal conglomerate.  Mx. thickness: 610m.  Geological Province: Mount Painter Province.||||||
10317|Leigh Creek Coal Measures|30176|6|Mentioned|Map legend|Jurassic|Triassic|Triassic - Jurassic age||||||
10317|Leigh Creek Coal Measures|30455|6|Mentioned|p13|||See alsp P17,18,21. Jurassic age||||||
10317|Leigh Creek Coal Measures|30458|6|Mentioned|p3|||Liassic.||||||
10317|Leigh Creek Coal Measures|30460|6|Mentioned|p5|||See also P12-16,22. Rhaetian - Triassic age||||||
10317|Leigh Creek Coal Measures|30465|6|Mentioned|p1|||||||||
10317|Leigh Creek Coal Measures|30466|6|Mentioned|p5|||Jurassic.||||||
10317|Leigh Creek Coal Measures|30475|6|Mentioned|p168|||||||||
10317|Leigh Creek Coal Measures|30512|6|Mentioned|p45|||||||||
10317|Leigh Creek Coal Measures|30565|6|Mentioned|Fig.10|||||||||
10317|Leigh Creek Coal Measures|32136|6|Mentioned|p5|||Miospores||||||
10317|Leigh Creek Coal Measures|32803|6|Mentioned|p96|||||||||
10317|Leigh Creek Coal Measures|34010|6|Mentioned|Cor. chart|||U. Triassic||||||
10317|Leigh Creek Coal Measures|34287|6|Mentioned|p151|||Triassic||||||
10317|Leigh Creek Coal Measures|34611|4|Described|p136|||Upper Triassic (Rhaetic) - Lower Jurassic (Lias). See Fig.61.||||||
10317|Leigh Creek Coal Measures|35901|6|Mentioned|p5|||||||||
10317|Leigh Creek Coal Measures|36081|4|Described|p444|||||||||
10317|Leigh Creek Coal Measures|36327|6|Mentioned|p5|||||||||
10317|Leigh Creek Coal Measures|36899|6|Mentioned|p1095|||||||||
10317|Leigh Creek Coal Measures|37065|6|Mentioned|p38|||||||||
10317|Leigh Creek Coal Measures|37812|6|Mentioned|p657|||||||||
10317|Leigh Creek Coal Measures|38068|6|Mentioned|p71|||||||||
10317|Leigh Creek Coal Measures|39352|6|Mentioned|Map legend|Triassic|Triassic|||||||
10317|Leigh Creek Coal Measures|41535|6|Mentioned|Fig.2|||||||||
10317|Leigh Creek Coal Measures|42008|6|Mentioned|p266|||||||||
10317|Leigh Creek Coal Measures|42713|5|Briefly described|Fig. P18|||||||||
10317|Leigh Creek Coal Measures|42746|6|Mentioned|p8|||See also P36.||||||
10317|Leigh Creek Coal Measures|43052|5|Briefly described|Table 2.1|||||||||
10317|Leigh Creek Coal Measures|43053|5|Briefly described|Map Legend|Jurassic|Jurassic|||||||25-MAY-05
10317|Leigh Creek Coal Measures|43258|5|Briefly described|Map Legend|Jurassic|Triassic|||||||
10317|Leigh Creek Coal Measures|43298|5|Briefly described|Map Legend|Jurassic|Triassic|||||||12-MAY-17
10317|Leigh Creek Coal Measures|43910|14|Not recorded|p12|Lias|Rhaetian|||||||
10317|Leigh Creek Coal Measures|43923|6|Mentioned|p15|||||||||
10317|Leigh Creek Coal Measures|43924|14|Not recorded|p2,3|Lias|Rhaetian|(Rhaeto-Liassic age)||||||
10317|Leigh Creek Coal Measures|44029|14|Not recorded|p157|Lias|Rhaetian|Rhaetic-Liassic plant.||||||
10317|Leigh Creek Coal Measures|44030|14|Not recorded|p126,140|Lias|Rhaetian|||||||
10317|Leigh Creek Coal Measures|44133|5|Briefly described|p93, 96, 98|Upper Triassic|Triassic|Geological Province: Eromanga Basin. Thickness: >1500m.||||||
10317|Leigh Creek Coal Measures|60953|5|Briefly described|Map Legend|Jurassic|Triassic|Fluvial and lacustrine carbonaceous mudstone, coal, siltstone and sandstone.||||||
10317|Leigh Creek Coal Measures|60991|6|Mentioned|p46 |||Contains leaves of the Rochipteris genus, previously ascribed to Ginkgophytopsis.||||||12-MAY-17
10317|Leigh Creek Coal Measures|61108|5|Briefly described|map legend|Jurassic|Triassic|Fluvial and lacustrine carbonaceous mudstone, coal, siltstone and sandstone.||||||
10317|Leigh Creek Coal Measures|63936|6|Mentioned|p191|||Playford and Dettman (1965). Significant palynological change over the Triassic-Jurassic boundary, similar to the northern Carnarvon Basin.||||||
10317|Leigh Creek Coal Measures|63979|6|Mentioned|p30|||Of Powis (1989).||||||07-FEB-11
10317|Leigh Creek Coal Measures|65313|6|Mentioned|p577|Triassic|Triassic|Over 610 m thick. Include sub-bituminous coals.||||||
10317|Leigh Creek Coal Measures|68135|6|Mentioned|p49|Early Jurassic|Late Triassic|South Australia. Isolated deposits. Time span is given as Rhaeto-Liassic.||||||
10343|Lennis Sandstone|22707|5|Briefly described|P15||Early Paleozoic|||||||07-NOV-08
10343|Lennis Sandstone|23571|5|Briefly described|p22|||See also Lennis Formation. Shallow marine shale and sandstone. Geological Province: Officer Basin||||||16-MAY-05
10343|Lennis Sandstone|23858|5|Briefly described|p919|Early Permian|Cambrian|Geological Province: Officer Basin.||||||
10343|Lennis Sandstone|24067|5|Briefly described|p250|Cambrian|Cambrian|Geological Province: Officer Basin.||||||
10343|Lennis Sandstone|24161|4|Described|p9 Fig.6, p29|Devonian|Devonian|Unconformably overlies the Table Hill Volcanics. Unconformably overlain by the Wanna Formation. Geological Province: Gunbarrel Basin.||||||
10343|Lennis Sandstone|24390|5|Briefly described|p11 Fig. 6|Devonian|Silurian|Geological Province: Gunbarrel Basin.||||||
10343|Lennis Sandstone|31455|6|Mentioned|p12|||||||||
10343|Lennis Sandstone|31456|4|Described|Table 2|||||||||
10343|Lennis Sandstone|31457|4|Described|Table 2|||||||||
10343|Lennis Sandstone|31459|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
10343|Lennis Sandstone|31460|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
10343|Lennis Sandstone|31562|5|Briefly described|p9|||Refers Lennis et al. (1972)||||||
10343|Lennis Sandstone|31632|4|Described|Table 2|||See also p11.||||||06-SEP-18
10343|Lennis Sandstone|31633|4|Described|Table 2|||Mention p7.||||||06-SEP-18
10343|Lennis Sandstone|31634|4|Described|Table 1|||||||||
10343|Lennis Sandstone|31635|4|Described|Table 2|||||||||
10343|Lennis Sandstone|31636|5|Briefly described|p7|||See Table 2.||||||
10343|Lennis Sandstone|31638|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
10343|Lennis Sandstone|31639|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
10343|Lennis Sandstone|31640|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
10343|Lennis Sandstone|31641|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
10343|Lennis Sandstone|31642|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
10343|Lennis Sandstone|31914|2|Defined|p96|Carboniferous|Silurian|Ordovician to U.Carb.||||||
10343|Lennis Sandstone|32586|5|Briefly described|p114|||Refers Jackson (1966) p111.||||||06-SEP-18
10343|Lennis Sandstone|32648|6|Mentioned|p32|||Ludlovian||||||
10343|Lennis Sandstone|33586|4|Described|Table 1|||See also p12.||||||06-SEP-18
10343|Lennis Sandstone|33590|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
10343|Lennis Sandstone|33591|5|Briefly described|p8|||||||||
10343|Lennis Sandstone|33592|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
10343|Lennis Sandstone|33595|4|Described|Table 1|||||||||
10343|Lennis Sandstone|34417|6|Mentioned|p97|||||||||
10343|Lennis Sandstone|35123|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
10343|Lennis Sandstone|36096|6|Mentioned|Fig.3|||||||||
10343|Lennis Sandstone|36257|6|Mentioned|Table 2.1|||||||||
10343|Lennis Sandstone|36701|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
10343|Lennis Sandstone|36889|5|Briefly described|p219|||||||||
10343|Lennis Sandstone|36890|3|Fully described|p404|||||||||
10343|Lennis Sandstone|38329|6|Mentioned|p202|||||||||
10343|Lennis Sandstone|38898|6|Mentioned|Table 1|||||||||
10343|Lennis Sandstone|41276|6|Mentioned|p75|||||||||
10343|Lennis Sandstone|42030|5|Briefly described|p750|||||||||
10343|Lennis Sandstone|42734|5|Briefly described|map legend|Devonian||||||||
10343|Lennis Sandstone|44354|5|Briefly described|Map Legend||Early Permian|||||||
10343|Lennis Sandstone|45149|2|Defined|p39|Carboniferous|Silurian|Early Cambrian to Early Permian. See also Table 1 and Fig.12.||||||
10343|Lennis Sandstone|45168|6|Mentioned|Table 1|||See also p6.||||||
10343|Lennis Sandstone|46975|6|Mentioned|p86|||||||||
10343|Lennis Sandstone|49792|5|Briefly described|Fig.5|||||||||
10343|Lennis Sandstone|50085|5|Briefly described|p11 Fig. 6|Ordovician|Ordovician|Age: <500Ma.  Geological Province: Officer Basin.||||||
10343|Lennis Sandstone|50205|5|Briefly described|p59 Fig.1,|Devonian|Devonian|Of Gunbarrel Basin.||||Is overlain unconformably by Wanna Formation.||
10343|Lennis Sandstone|61023|5|Briefly described|p15 Fig. 8|Ordovician|Ordovician|Geological Province: Gunbarrel Basin.||||||11-APR-08
10343|Lennis Sandstone|61272|6|Mentioned|p120 Fig.1|||See also Lennis Formation.||||||29-NOV-06
10343|Lennis Sandstone|62453|6|Mentioned|p6 Fig. 4, 22|||See also Lennis Formation? Overlies: Table Hill Volcanics.||||||
10343|Lennis Sandstone|64325|5|Briefly described|p82 Fig. 2|Middle Devonian|Early Devonian|Geological Province: Gunbarrel  Basin.||||||26-AUG-08
10343|Lennis Sandstone|64580|4|Described|map legend||Ordovician|Fine- to medium-grained feldspathic micaceous sandstone, minor siltstone.||||||09-DEC-08
10343|Lennis Sandstone|64793|6|Mentioned|p286 Fig.5|Paleozoic|Paleozoic|||||||
10343|Lennis Sandstone|64970|6|Mentioned|p719, p719 Fig. 2, p720, p721 Fig. 6, 7|Devonian|Devonian|Geological Province: Officer Basin.||||||27-MAY-09
10343|Lennis Sandstone|65102|4|Described|p.366,370,373, 374, Figs4-41,4-49|Carboniferous|Late Devonian|Officer Basin. 50-425m; disconformable on Table Hill Volcanics, conformably overlain by Wanna Formation; red, fine to medium grained sandstone, commonly micaceous; micaceous siltstone interbeds; shallow marine but with some subaerial exposure; possibly also fluvial.||||||
10343|Lennis Sandstone|65363|6|Mentioned|p5 Fig.4, pp12-14, p19.|Ordovician|Ordovician|Shown repeatedly in this report as Lennis / Durba Sandstone, presumably for reasons of space. Southern Officer Basin. May correlate with Durba Sandstone in the northwest of the basin. Shown as Lennis Fm in Fig. 4, p5.||||Overlies Table Hill Volcanics. Is unconformably overlain by Paterson Formation.||
10343|Lennis Sandstone|65416|5|Briefly described|p137, p138 Fig.3, p139 Fig.4, pp144-146.|Early Carboniferous|Devonian|Officer Basin. Part of Sequence Pz4. Sandstone and claystone betweeen 100 and 465 m in Hussar 1, previously interpreted as Lennis Sandstone and Wanna Formation, are now included in Durba Sandstone. Age from fission-track analysis. Also called Lennis Formation on p145.||||Unconformably overlies Table Hill Volcanics and Browne Formation. Is overlain unconformably by Paterson Formation.||
10343|Lennis Sandstone|67195|5|Briefly described|p10 fig 6, p19 table 1,p40, p44, 47|Devonian|Devonian|Gunbarrel Basin. Probably misspelt as Lennis Formation in Fig 5 p9. Thermal conductivity of 2.60 W/mK. Basal unit of one well in this study. See also App 1, App 2.||||Unconformably overlain by Wanna Formation, Unconformably overlies Table Hill Volcanics|Partially friable, yellow medium grained sandstone.|
10343|Lennis Sandstone|67200|5|Briefly described|app 2 p8||||||||Partially friable medium grained sandstone.|
10343|Lennis Sandstone|69029|6|Mentioned|p329|Devonian|Devonian|Of Officer Basin.||||Overlain unconformably by Wanna Formation. Underlain unconformably by Table Hill Volcanics.||
10343|Lennis Sandstone|69091|5|Briefly described|p30 Fig.3.5, p37, see comments|Ordovician|Cambrian|Officer Basin. Misspelt as Lenis Sandstone on p44. Unconstrained as to age, but appears to be aeolian at least in part. See also p38 Fig.3.7, p41 Fig.3.8, p44, p81 Fig.4.17, p108 Fig.5.9, p174 Fig.9.5, p177 Fig.9.6, p200 Fig.10.2.||||Overlies Table Hill Volcanics; is overlain by Paterson Formation.||
10343|Lennis Sandstone|69153|6|Mentioned|500k_geologyp08_lut.csv||Ordovician||||||Fine- to medium-grained feldspathic micaceous sandstone, minor siltstone|
10343|Lennis Sandstone|70634|4|Described|500k_geolgyp08_lut.csv|Ordovician|Ordovician||||||Fine- to medium-grained feldspathic micaceous sandstone, minor siltstone.|
10343|Lennis Sandstone|70793|4|Described|500k_interpgeop14_lut.csv|Ordovician|Series 3|Of Officer Basin (Phase 2). Events: Gondwana breakup-southern margin (100.5-93.9 Ma); Rodingan Movement (Alice Springs Orogeny phase 1) (450-420 Ma). See 500k_interpgeop14_lut.csv, 2_5m_interpgeop15_lut.csv.|509-443.4 Ma (inferred)||||Fine- to medium-grained feldspathic micaceous sandstone, minor siltstone; giant cross beds, possibly eolian|
10343|Lennis Sandstone|70826|6|Mentioned|p7 tbl 3|Ordovician|Cambrian|Officer Basin.||||||
10343|Lennis Sandstone|71146|5|Briefly described|p6, p26|Early Ordovician|Furongian|Officer Basin.||||Unconformably overlies the Table Hill Volcanics. Unconformably overlain by the Wanna Formation.|Sandstone.|
10343|Lennis Sandstone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone|
10343|Lennis Sandstone|71268|4|Described|GEOL_LUT_CSV files|Ordovician|Series 3|Of Officer Basin (Phase 2). Events: Gondwana breakup-southern margin (100.5-93.9 Ma); Rodingan Movement (Alice Springs Orogeny phase 1) (450-420 Ma). See 250k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 1m_geologyp12_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv.|508-443.4 Ma (inferred)||||Fine- to medium-grained, feldspathic, micaceous sandstone; minor siltstone; giant cross-beds, possibly eolian|
10343|Lennis Sandstone|71618|6|Mentioned|p130|||Of Officer Basin.||||||
10343|Lennis Sandstone|71800|6|Mentioned|p26-p27|Middle Ordovician|Early Ordovician|Officer Basin.|||||Feldspathic sandstone.|
10343|Lennis Sandstone|72034|5|Briefly described|500k_interpgeop16_lut|Ordovician|Series 3|Officer Basin (Phase 2).|||||Fine- to medium-grained feldspathic micaceous sandstone, minor siltstone; giant cross beds, possibly eolian.|
10343|Lennis Sandstone|73346|6|Mentioned|p25|||Officer Basin.||||||
10358|Levenger Formation|23282|6|Mentioned|p68|||||||||
10358|Levenger Formation|31970|4|Described|p15|||Torrensian?||||||
10358|Levenger Formation|43052|5|Briefly described|Table 2.1|||||||||
10358|Levenger Formation|43053|5|Briefly described|Map Legend|Cambrian|Cambrian|Conglomerate, arkose, shale, siltstone.||||||25-MAY-05
10358|Levenger Formation|43258|5|Briefly described|Map Legend||Cambrian|||||||
10358|Levenger Formation|43298|6|Mentioned|Map Legend||Cambrian|||||||
10358|Levenger Formation|44133|5|Briefly described|p38-39|Middle Paleozoic|Early Paleozoic|||||||07-NOV-08
10358|Levenger Formation|60953|5|Briefly described|Map Legend|Cambrian|Cambrian|Conglomerate, arkose, shale, siltstone.||||||
10358|Levenger Formation|61108|5|Briefly described|map legend|Cambrian|Cambrian|Conglomerate, arkose, shale and siltstone.||||||06-JUN-05
10358|Levenger Formation|65376|5|Briefly described|p9 Fig.1.2. |Paleozoic|Paleozoic||||||Conglomerate, arkose, shale, siltstone.|
10358|Levenger Formation|67536|6|Mentioned|Map Legend|||Levenger Graben.|||||Pebble conglomerate, arkose, quartzite, minor siltstone and dolomite.|
10358|Levenger Formation|68131|5|Briefly described|p2 Fig.1|Cambrian|Cambrian|Mapped with Moorilyanna Conglomerate as a single unit.|||||Conglomerate, arkose, shale and siltstone.|
10358|Levenger Formation|70839|5|Briefly described|p345|||Occurs in Levenger 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.||||||
10521|Llewellin Sandy Loam|38290|5|Briefly described|p62|||||||||
10622|Long Gully Member|40448|5|Briefly described|Table 3|||||||||
10631|Longford Limestone|24551|6|Mentioned|p608|||Of the Gippsland Limestone||||||
10631|Longford Limestone|31351|6|Mentioned|p86|||||||||
10631|Longford Limestone|31850|6|Mentioned|p36|||Refers Carter (1964)||||||
10631|Longford Limestone|33459|6|Mentioned|Table 1|||||||||
10631|Longford Limestone|34421|6|Mentioned|p259|||||||||
10631|Longford Limestone|38070|6|Mentioned|Fig.12|||Gippsland Basin||||||
10631|Longford Limestone|44215|14|Not recorded|p360|||||||||
10631|Longford Limestone|70076|5|Briefly described|Regional: Fig.3|Langhian|Aquitanian|||Seaspray Group.||Overlies Lakes Entrance Formation. Is overlain by Wuk Wuk Marl.||
10640|Longsight Sandstone|29591|6|Mentioned|Table 72|||||||||
10640|Longsight Sandstone|29961|4|Described|p12|||Cretaceous||||||
10640|Longsight Sandstone|30021|6|Mentioned|p87|||||||||
10640|Longsight Sandstone|30102|4|Described|p26|||See also P17,27,28,29.||||||
10640|Longsight Sandstone|30461|6|Mentioned|p100|||||||||
10640|Longsight Sandstone|30914|6|Mentioned|Map legend|Cretaceous|Jurassic|Jurassic - Cretaceous||||||
10640|Longsight Sandstone|31572|4|Described|Fig. 1|||L.Cretaceous||||||
10640|Longsight Sandstone|32275|6|Mentioned|p8|||Refers Casey (1959)||||||
10640|Longsight Sandstone|32576|6|Mentioned|p51|||||||||
10640|Longsight Sandstone|33073|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
10640|Longsight Sandstone|33075|6|Mentioned|p451|||Refers Casey (1959)||||||
10640|Longsight Sandstone|33111|4|Described|p43|||Mention P6.||||||
10640|Longsight Sandstone|33164|6|Mentioned|Fig.4|||||||||
10640|Longsight Sandstone|33165|6|Mentioned|Chart|||Correlation chart only||||||
10640|Longsight Sandstone|33414|6|Mentioned|p212-214,Tb.||Neocomian|||||||
10640|Longsight Sandstone|33638|6|Mentioned|p10|||||||||
10640|Longsight Sandstone|33825|6|Mentioned|p10|||Correlation table||||||
10640|Longsight Sandstone|33964|6|Mentioned|p6|||Refers Casey (1968) & Yeates (1971).||||||
10640|Longsight Sandstone|34454|5|Briefly described|Table 2|||L.Cret.||||||
10640|Longsight Sandstone|34619|6|Mentioned|p.160, Pl.22||Cretaceous|||||||08-APR-13
10640|Longsight Sandstone|34847|6|Mentioned|p37|||||||||
10640|Longsight Sandstone|35121|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
10640|Longsight Sandstone|35139|4|Described|Table.2|||||||||
10640|Longsight Sandstone|35811|6|Mentioned|p556|||Exploration carried out.||||||
10640|Longsight Sandstone|39211|6|Mentioned|p26|||||||||
10640|Longsight Sandstone|39445|5|Briefly described|Table 10|||||||||
10640|Longsight Sandstone|41125|6|Mentioned|p42|||||||||
10640|Longsight Sandstone|41247|6|Mentioned|p126|||||||||
10640|Longsight Sandstone|42397|6|Mentioned|Fig.2 P3|||||||||
10640|Longsight Sandstone|42447|6|Mentioned|p5 + Fig. 17|||Part equivalent to Westbourne Formation.||||||
10640|Longsight Sandstone|42474|5|Briefly described|p26|||||||||
10640|Longsight Sandstone|42749|5|Briefly described|p31|||see also Fig.2 P27||||||
10640|Longsight Sandstone|43105|5|Briefly described|Fig.9,p15|||||||||
10640|Longsight Sandstone|43122|5|Briefly described|p23|||see also Fig. 2.||||||
10640|Longsight Sandstone|43883|14|Not recorded|p18 Fig.4-3|||||||||
10640|Longsight Sandstone|43985|4|Described|p8,10-13,Fig.3,Pl.2|||||||||
10640|Longsight Sandstone|44031|14|Not recorded|p5,8|Cretaceous|Jurassic|||||||
10640|Longsight Sandstone|44082|6|Mentioned|Table p34||Aptian|Mention on correlation table of Queensland Cretaceous sediments.||||||
10640|Longsight Sandstone|44087|14|Not recorded|p4,7,opp.7|||||||||
10640|Longsight Sandstone|44119|14|Not recorded|Map Legend|Early Cretaceous|Late Jurassic|||||||
10640|Longsight Sandstone|44120|14|Not recorded|Map Legend|Early Cretaceous|Late Jurassic|||||||
10640|Longsight Sandstone|44121|14|Not recorded|p5-6,10-12|Early Cretaceous|Late Jurassic|||||||
10640|Longsight Sandstone|44122|2|Defined|p318-323,Fig.48|||||||||
10640|Longsight Sandstone|44168|4|Described|Tb.1,6,5,10,map|||||||||
10640|Longsight Sandstone|44212|14|Not recorded|p110|||Not on white card.||||||
10640|Longsight Sandstone|44276|4|Described|p25,Tb.2,map|||Aquifer.||||||
10640|Longsight Sandstone|44277|14|Not recorded|Map Legend||Early Cretaceous|||||||
10640|Longsight Sandstone|44291|2|Defined|Tb.1,p6,8,13,14,map||Early Cretaceous|Equivalent to upper part of Blythesdale Group.||||||
10640|Longsight Sandstone|44308|14|Not recorded|p2,11,13,Tb.2||Early Cretaceous|||||||
10640|Longsight Sandstone|44309|2|Defined|Tb.1,p7,13,14,map|||||||||
10640|Longsight Sandstone|44310|14|Not recorded|Map Legend||Early Cretaceous|||||||
10640|Longsight Sandstone|44312|14|Not recorded|Map Legend||Early Cretaceous|||||||
10640|Longsight Sandstone|44326|14|Not recorded|Map Legend||Early Cretaceous|||||||
10640|Longsight Sandstone|44346|14|Not recorded|p4,5,10|||||||||
10640|Longsight Sandstone|44361|14|Not recorded|Map Legend||Early Cretaceous|||||||
10640|Longsight Sandstone|44362|4|Described|p11,Tb.1||Early Cretaceous|||||||
10640|Longsight Sandstone|44376|14|Not recorded|p4,5|||||||||
10640|Longsight Sandstone|44406|14|Not recorded|p4,opp.p6|||||||||
10640|Longsight Sandstone|44408|14|Not recorded|p4,opp.p6|||||||||
10640|Longsight Sandstone|44469|2|Defined|opp.p.6,p.12, Tb.I||Cretaceous|(F53-12). Rhizocorallium, wood.||||||
10640|Longsight Sandstone|44470|5|Briefly described|map legend||Cretaceous|||||||02-DEC-04
10640|Longsight Sandstone|44543|2|Defined|p34,36||Early Cretaceous|Underlies Wilgunyah Formation.||||||
10640|Longsight Sandstone|44611|14|Not recorded|p22|||||||||
10640|Longsight Sandstone|44634|14|Not recorded|p30|||||||||
10640|Longsight Sandstone|44920|14|Not recorded|Map Legend,Sheet 4||Cretaceous|||||||
10640|Longsight Sandstone|45004|14|Not recorded|p.8,20,32,36,38-63|||On many pages.||||||
10640|Longsight Sandstone|45051|6|Mentioned|Fig.2A|||Lower Cretaceous. See also Fig.5A, 3.||||||
10640|Longsight Sandstone|45052|5|Briefly described|p134|||Cretaceous||||||
10640|Longsight Sandstone|45094|6|Mentioned|p9|||Cret.||||||
10640|Longsight Sandstone|45103|6|Mentioned|p5|||||||||
10640|Longsight Sandstone|48906|14|Not recorded|p5,Tb.2,App.C,Pl.1|Early Cretaceous|Late Jurassic|||||||
10640|Longsight Sandstone|48908|14|Not recorded|Tb.1||Early Cretaceous|||||||
10640|Longsight Sandstone|49027|5|Briefly described|p21|||||||||
10640|Longsight Sandstone|60122|5|Briefly described|p35|Cretaceous|Cretaceous|Subsumed into Hooray Sandstone, together with the Tarlton Formation (Mond and Harrison, in Senior et al 1978).||||||
10640|Longsight Sandstone|63450|5|Briefly described|p83|Cretaceous|Jurassic|As defined by Casey (1959) contained two distinct facies, a lower fluvial facies and upper glauconitic marine facies. The latter may be equivalent to Cadna-owie Formation.||||||08-APR-13
10640|Longsight Sandstone|66915|5|Briefly described|p9, p11 Fig.7|||Western Eromanga Basin.||||Is overlain by Wallumbilla Formation on western margin of Eromanga Basin, at C-horizon boundary.||
10640|Longsight Sandstone|67323|5|Briefly described|GIS attrib tbl, p92 Fig.12.2|Cretaceous|Jurassic|See also Solid Geology Map. Galilee/Eromanga/Carpentaria Basins.||||Overlies Ethabuka Sandstone. Is overlain by Wallumbilla Formation.|Sandstone, ferruginous sandstone, conglomerate, some siltstone.|
10640|Longsight Sandstone|67402|6|Mentioned|p214|Cretaceous|Cretaceous|Aquifer unit.||||||
10640|Longsight Sandstone|68553|6|Mentioned|Map legend; schematic diagram.|Early Cretaceous|Jurassic|Surat Basin. This unit, as well as Bungil, Orallo and Southlands Formations; Gubberamunda, Hooray and Mooga Sandstones, and Kumbarilla beds, are all mapped under the symbol, JKb.||||||
10640|Longsight Sandstone|69457|5|Briefly described|p41:6|||This name was applied (Smith 1963, 1965; Mond and Harrison in Senior et al. 1978) to outliers of Eromanga Basin strata in TOBERMOREY and HAY RIVER map areas. Some were remapped as undifferentiated Jurassic-Cretaceous by Kruse et al. (2002). They are most probably equivalents of the Algebuckina Sandstone (and possibly the Cadna-owie Formation).|||||Mesa-forming planar to cross-bedded, medium-coarse sandstone and minor mudstone, siltstone and conglomerate.|12-JUL-16
10640|Longsight Sandstone|69594|5|Briefly described|p526, p528|Barremian|Callovian|NW Eromanga Basin. Includes outliers of nominally Mesozoic sedimentary rocks that overlie elements of the Georgina Basin and Precambrian Mount Isa Province. Has been correlated with all units ranging from Hutton Sandstone to Wallumbilla Formation.||||Is overlain by Wallumbilla Formation.||
10656|Loongana Formation|22613|6|Mentioned|p18|||||||||
10656|Loongana Formation|22663|5|Briefly described|S97-1 and 2 p3||Early Cretaceous|||||||01-MAR-10
10656|Loongana Formation|42075|5|Briefly described|Fig.10 P250|||||||||
10656|Loongana Formation|42545|1|Redefined|p13|Hauterivian|Berriasian|||||||
10656|Loongana Formation|43026|5|Briefly described|Table 1,p586|||||||||
10656|Loongana Formation|43052|5|Briefly described|Table 2.1|||||||||
10656|Loongana Formation|44133|5|Briefly described|p134|Hauterivian|Valanginian|Conformably overlain by Madura Formation. Originally named 'Loongana Conglomerate'.||||||
10656|Loongana Formation|45149|6|Mentioned|Table 1|||Page 15.||||||
10656|Loongana Formation|61630|6|Mentioned|p555 Fig. 3|Early Cretaceous|Late Jurassic|Geological Province: Eyre Sub-basin.||||||07-APR-09
10656|Loongana Formation|64580|4|Described|map legend||Early Cretaceous|Cross-bedded feldspathic sandstone, locally conglomeratic, carbonaceous sandstone; glauconitic sandstone, siltstone, claystone and shale; commonly pyritic.||||||09-DEC-08
10656|Loongana Formation|68715|6|Mentioned|p30 Fig.5|Hauterivian|Berriasian|Bight Basin.||||||
10656|Loongana Formation|69297|5|Briefly described|p14 fig 2.4, p25 fig 2.9, p60|Hauterivian|Berriasian|Eyre Sub-basin.||||Overlain by the Madura Formation.|Sandstone, siltstone and shale.|
10656|Loongana Formation|69632|5|Briefly described|p21 Tb.6, p26, p30, p32|Cretaceous|Cretaceous|Gunbarrel, Eucla Basins. Average shear-wave velocities tabulated. 27-49m thick.||Bight Basin Group.||Is overlain by Madura Formation.|A lenticular, conglomeratic, feldspathic, grey-bluish sandstone. Largely unconsolidated and poorly lithified.|
10656|Loongana Formation|69648|4|Described|p20-21, map legend|Early Cretaceous|Early Cretaceous|Of Bight Basin margin. Occurs in drillholes. Thickness: about 18.3 m. Fluviatile continental deposition.||||Disconformably overlain by Madura Formation.|An essentially sandstone unit; ferruginous gradational, cyclically deposited conglomerates and sandstones through to fine clayey silts; may include mud, and be carbonaceous.|
10656|Loongana Formation|70771|5|Briefly described|p2, p27|Cretaceous|Cretaceous|Eucla Basin.||||Conformably overlain by the Madura Formation.|Siliciclastic sedimentary rocks.|
10656|Loongana Formation|70772|4|Described|p2, p4-9, p11-12, p16-17|Hauterivian|Valanginian|Madura Shelf. Nonconformably overlies crystalline basement. Intersected in nine wells and achieves a thickness between 20 and 43m. Petrography is discussed further. Deposited in a high-energy fluvial/lacustrine type environment. Poor sorting and textural immaturity suggest deposition was rapid. Palynology suggests a freshwater/brackish type setting. See also p22-24, p28, p31, p33-34, p36, p41.||||Conformably overlain by the Madura Formation. Disconformably overlies the Decoration Sandstone.|Very poorly consolidated, quartz dominated, feldspathic sand with minor mica. Medium-coarse grained, angular, poorly sorted sand.|
10656|Loongana Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone|
10656|Loongana Formation|71618|4|Described|p124-125,127-135|Hauterivian|Valanginian|Geological province: Bight Basin, Madura Shelf. Deposited during period of thermal subsidence during the Early Cretaceous. Intersected in 9 wells in the study area. Thickness: 20-40m. Sample in the FOR010 borehole (235.9-235.92 m and 244.3-244.5 m) contained a distinctive and rich Early Cretaceous palynomorph assemblage (see p127 for palynology). U-Pb ICPMS zircon analysis yield major concordant age peaks at c. 1150 and 1650 Ma, similar to the Decoration Sandstone and Madura Formation.||||Conformably overlain by Madura Formation. Underlain by crystalline basement, or Decoration Sandstone where present.|Very poorly consolidated quartz dominated, feldspathic sand with minor mica.|06-SEP-19
10656|Loongana Formation|71891|5|Briefly described|p6-p7, p14, p29, p32-p33, |Early Cretaceous|Middle Jurassic|Bight Basin, Coompana Province. 30-324m thick. Interpreted to represent the initial rift phase of the basin. Deposited in a terrestrial low sinuosity fluvial environment. See also p35-p37, p44-p52, p54-p55.||||Conformably overlain by the Madura Formation.|Semi-solid sand, pebly conglomerate.|
10656|Loongana Formation|72344|5|Briefly described|p4, p9, p13, p49, p61|Early Cretaceous|Early Cretaceous|Bight Basin. Maximum thickness of 324m. Interpreted to represent an initial rift phase in a terrestrial low sinuosity fluvial environment. Intersected in drillhole CDP008. Petrography, SHRIMP analyses and geochemistry are discussed for several samples.Maximum depositional age is derived from SHRIMP dating in this volume. See also p84, p107, p110-p112, p125, p169.|350 +/- 5 (max dep age)|||Conformably overlain by the Madura Formation.|Sandy to shaly succession of cross-bedded feldspathic sandstone, locally conglomeratic, carbonaceous sandstone; glauconitic sandstone, siltstone, claystone and shale; commonly pyritic.|
10656|Loongana Formation|72465|5|Briefly described|p8|Early Cretaceous|Early Cretaceous|Hill (1991, 1995). Bight Basin, Coompana Province. Represents an initial rift phase in a terrestrial low-sinuosity fluvial environment within isolated grabens. Up to 324m thick.||||Is overlain by Madura Formation.|Cross-bedded feldspathic sandstone, locally conglomeratic, carbonaceous; glauconitic sandstone, siltstone, claystone and shale; commonly pyritic.|
10656|Loongana Formation|72466|5|Briefly described|p8, 17|Early Cretaceous|Early Cretaceous|Hill (1991, 1995). Bight Basin, Coompana Province. Up to 324m thick. Represents an initial rift phase in a terrestrial low-sinuosity fluvial environment within isolated grabens.||||Is overlain conformably by Madura Formation.|Cross-bedded feldspathic sandstone, locally conglomeratic, carbonaceous sandstone; glauconitic sandstone, siltstone, claystone and shale; commonly pyritic.|
10656|Loongana Formation|72467|5|Briefly described|p8, 17|Early Cretaceous|Early Cretaceous|Hill (1991, 1995). Bight Basin, Coompana Province. Up to 324m thick. Represents an initial rift phase in a terrestrial low-sinuosity fluvial environment within isolated grabens.||||Overlies ?Moodini Supersuite. Is overlain conformably by Madura Formation.|Cross-bedded feldspathic sandstone, locally conglomeratic, carbonaceous sandstone; glauconitic sandstone, siltstone, claystone and shale; commonly pyritic.|
10656|Loongana Formation|72468|5|Briefly described|p8, p17|Early Cretaceous|Early Cretaceous|Bight Basin. Maximum thickness of 324 m. Interpreted to represent an initial rift phase in a terrestrial low-sinuosity fluvial environment within isolated grabens of the developing rift valley.||||Conformably overlain by Madura Formation.|Cross-bedded feldspathic sandstone, locally conglomeratic, carbonaceous sandstone; glauconitic sandstone, siltstone, claystone and shale; commonly pyritic.|
10656|Loongana Formation|72469|5|Briefly described|p8, p17|Early Cretaceous|Early Cretaceous|Bight Basin. Maximum thickness of 324 m. Interpreted to represent an initial rift phase in a terrestrial low-sinuosity fluvial environment within isolated grabens of the developing rift valley.||||Conformably overlain by Madura Formation.|Cross-bedded feldspathic sandstone, locally conglomeratic, carbonaceous sandstone; glauconitic sandstone, siltstone, claystone and shale; commonly pyritic.|
10656|Loongana Formation|72470|5|Briefly described|p8|Early Cretaceous|Early Cretaceous|Bight Basin. Maximum thickness of 324 m. Interpreted to represent an initial rift phase in a terrestrial low-sinuosity fluvial environment within isolated grabens of the developing rift valley.||||Conformably overlain by Madura Formation.|Cross-bedded feldspathic sandstone, locally conglomeratic, carbonaceous sandstone; glauconitic sandstone, siltstone, claystone and shale; commonly pyritic.|
10656|Loongana Formation|72471|5|Briefly described|p8|Early Cretaceous|Early Cretaceous|Bight Basin. Maximum thickness of 324 m. Interpreted to represent an initial rift phase in a terrestrial low-sinuosity fluvial environment within isolated grabens of the developing rift valley.||||Conformably overlain by Madura Formation.|Cross-bedded feldspathic sandstone, locally conglomeratic, carbonaceous sandstone; glauconitic sandstone, siltstone, claystone and shale; commonly pyritic.|
10656|Loongana Formation|72472|5|Briefly described|p8, p17-18, p20-21|Early Cretaceous|Early Cretaceous|Bight Basin. Maximum thickness of 324 m. Interpreted to represent an initial rift phase in a terrestrial low-sinuosity fluvial environment within isolated grabens of the developing rift valley. Interfingering transition with overlying Madura Formation.||||Conformably overlain by Madura Formation.|Cross-bedded feldspathic sandstone, locally conglomeratic, carbonaceous sandstone; glauconitic sandstone, siltstone, claystone and shale; commonly pyritic.|
10656|Loongana Formation|72947|6|Mentioned|p16|Early Cretaceous|Early Cretaceous|||||Nonconformably underlain by Koonalda Suite.||
10656|Loongana Formation|73084|5|Briefly described|p16-17|Early Cretaceous|Early Cretaceous|Bight Basin. 10-50 m thick.||||Overlain by Madura Formation.|Poorly consolidated dark carbonaceous shale, siltstone and minor sandstone.|
10656|Loongana Formation|73641|5|Briefly described|p4, 8-15, 17|Early Cretaceous|Early Cretaceous|Bight Basin. ~30m thick. Terrestrial low-sinuosity fluvial environment within isolated grabens in a rift valley. Mineralogical, element, TOC compositions tabulated.||||Underlies and interfingers with Madura Formation.|Sandstones, carbonaceous sandstones, glauconitic sandstones, siltstones, and argillites, commonly pyritic.|
10684|Loveday Soil|23818|5|Briefly described|p212 Fig.108|Late Pleistocene|Late Pleistocene|||||||
10684|Loveday Soil|24176|5|Briefly described|p21, p22 Tb. 1|Pleistocene|Pleistocene|Of Pooraka Formation.  Geological Province: Mount Painter Province.||||||
10684|Loveday Soil|30056|6|Mentioned|Table 4|||||||||
10684|Loveday Soil|30176|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
10684|Loveday Soil|30751|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
10684|Loveday Soil|30752|6|Mentioned|p4|||||||||
10684|Loveday Soil|30753|6|Mentioned|p14|||Recent age||||||
10684|Loveday Soil|30755|6|Mentioned|p169|||Tectonic map||||||
10684|Loveday Soil|30756|6|Mentioned|p4|||||||||
10684|Loveday Soil|30802|6|Mentioned|p10|||Pleistocene age||||||
10684|Loveday Soil|30807|6|Mentioned|p101|||Suggested map symbol||||||
10684|Loveday Soil|30922|6|Mentioned|Map legend|Holocene|Holocene|||||||
10684|Loveday Soil|30994|6|Mentioned|p250|||Refers to Firman (1969)||||||
10684|Loveday Soil|31966|6|Mentioned|p6|||||||||
10684|Loveday Soil|32426|6|Mentioned|p142|||Stratigraphic table. Renmark area||||||
10684|Loveday Soil|32432|6|Mentioned|Fig.2|||See also Table 1||||||
10684|Loveday Soil|32561|6|Mentioned|p59|||See also Fig.4||||||
10684|Loveday Soil|33423|6|Mentioned|p15|||Strat.||||||
10684|Loveday Soil|33767|6|Mentioned|Fig.5|||||||||
10684|Loveday Soil|34180|6|Mentioned|p217|||Upper Pleistocene. See also P212||||||
10684|Loveday Soil|34536|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
10684|Loveday Soil|34758|6|Mentioned|Fig.2|||||||||
10684|Loveday Soil|35071|6|Mentioned|Fig.4|||||||||
10684|Loveday Soil|35200|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
10684|Loveday Soil|35232|6|Mentioned|Table.4|||||||||
10684|Loveday Soil|35673|6|Mentioned|Fig.1|||Location plan, Para Hills quartzite quarry.||||||
10684|Loveday Soil|35772|4|Described|Table 1|||||||||
10684|Loveday Soil|36626|6|Mentioned|Fig.1|||||||||
10684|Loveday Soil|36834|6|Mentioned|Fig.1|||||||||
10684|Loveday Soil|37853|6|Mentioned|Fig.1|||||||||
10684|Loveday Soil|38068|6|Mentioned|Fig.8|||||||||
10684|Loveday Soil|38107|6|Mentioned|p19|||||||||
10684|Loveday Soil|39349|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
10684|Loveday Soil|40442|6|Mentioned|p38|||||||||
10684|Loveday Soil|42717|5|Briefly described|map legend|Pleistocene||||||||
10684|Loveday Soil|42722|6|Mentioned|map legend|Pleistocene|Pleistocene|Developed locally in association with Wiabuna Formation.||||||07-APR-05
10684|Loveday Soil|43071|5|Briefly described|p17|||||||||
10684|Loveday Soil|43073|5|Briefly described|p18|||||||||
10684|Loveday Soil|44864|5|Briefly described|Map Legend||Pleistocene|||||||
10684|Loveday Soil|73112|5|Briefly described|Map legend.|Pleistocene|Pleistocene|Contained in the Woorinen Formation (equivalent).|||||Carbonate.|
10782|Lower Middleback Jaspilite|22629|6|Mentioned|p149|Paleoproterozoic|Paleoproterozoic|part of Hutchison Group (Middleback Subgroup).||||||07-NOV-08
10782|Lower Middleback Jaspilite|22851|5|Briefly described|13|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
10782|Lower Middleback Jaspilite|22854|6|Mentioned|P8||Paleoproterozoic|||||||07-NOV-08
10782|Lower Middleback Jaspilite|23719|4|Described|p14|Paleoproterozoic|Paleoproterozoic|See also p.14 Table 1. Of Middleback Subgroup. O'lying unit Cook Gap Schist. Underlying unit Katunga Dolomite. Geological Province: Gawler Craton. Max. thickness: >500 m.||||||07-NOV-08
10782|Lower Middleback Jaspilite|30806|5|Briefly described|p946|||||||||
10782|Lower Middleback Jaspilite|31034|6|Mentioned|Fig. 3|||||||||
10782|Lower Middleback Jaspilite|35298|5|Briefly described|p946|||||||||
10782|Lower Middleback Jaspilite|37811|2|Defined|p237|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
10782|Lower Middleback Jaspilite|39345|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
10782|Lower Middleback Jaspilite|39349|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
10782|Lower Middleback Jaspilite|39353|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
10782|Lower Middleback Jaspilite|41325|6|Mentioned|Fig.2|||||||||
10782|Lower Middleback Jaspilite|41327|6|Mentioned|Fig.2|||||||||
10782|Lower Middleback Jaspilite|41619|6|Mentioned|Map legend|Paleoproterozoic||||||||07-NOV-08
10782|Lower Middleback Jaspilite|42738|5|Briefly described|map legend|Paleoproterozoic||||||||07-NOV-08
10782|Lower Middleback Jaspilite|43052|5|Briefly described|p55|||of Middleback Subgroup||||||
10782|Lower Middleback Jaspilite|65376|6|Mentioned|p54. |||Name replaced by Middleback Subgroup.||||||
10782|Lower Middleback Jaspilite|65922|5|Briefly described|p14 Tb. 1, p15, 36|Orosirian|Orosirian|Gawler Craton. Of Middleback Subgroup, Hutchison Group. Interlayered down-sequence with Katunga Dolomite. Underlies Cook Gap Schist. Interlayered cherty to amphibolitic BIF and impure marble-calcsilicate.||||||
10782|Lower Middleback Jaspilite|66302|6|Mentioned|p24|||||Hutchison Group||||
10782|Lower Middleback Jaspilite|66882|5|Briefly described|p101, p103 Fig.3a,c|||Hosts massive iron ore deposits, mined since 19th Century.||Middleback Group.||Underlies Cook Gap Schist, overlies Katunga Dolomite.|Extensive BIF.|
10782|Lower Middleback Jaspilite|67536|6|Mentioned|Map Legend|||Gawler Craton.|||||Iron formation.|
10782|Lower Middleback Jaspilite|67721|5|Briefly described|p33, p33 Fig.2, p36, p38 Fig.9|||Between 120-450 m thick.||Of the Middleback Group.||Conformably overlain by the Cook Gap Schist.|Banded iron formation.|
10782|Lower Middleback Jaspilite|68158|6|Mentioned|p4|||||Hutchison Group.||||
10782|Lower Middleback Jaspilite|73026|5|Briefly described|p9|Paleoproterozoic|Paleoproterozoic|||||||
10782|Lower Middleback Jaspilite|73027|5|Briefly described|p9,|Palaeoproterozoic|Palaeoproterozoic||||||Amphibole-magnetite schist and quartzite.|
10820|Lowly Point Formation|40976|6|Mentioned|Table 1|||||||||
10820|Lowly Point Formation|44133|6|Mentioned|p228, 228 Fig. 11.7|||||||||
10820|Lowly Point Formation|62577|6|Mentioned|p566|Late Pleistocene|Late Pleistocene|||||||
10820|Lowly Point Formation|70334|4|Described|p3,61-64,66,70,83|||Of Spencer Gulf area. Thickness: 40cm to 4.15m thick on CULTANA. Not exposed on CULTANA, but intersected in vibrocores in Spencer Gulf where water depths exceed 14m. Transgressive marine unit, terminated by marine regression, sub-aerial exposire and pedogenesis. Contains a palaeosol defined by a weak calcareous horizon with slight clay enrichment, and the upper sandy horizons are truncated or reworked (Billing, 1984). Deposited in a narrow, protected ephemeral lagoonal environment, during a highstand after the last interglacial maximum (OIS 5a), at ~80 ka (Hails et al., 1984b).Overlain by modern alluvial sediments.||||Underlain by False Bay Formation. Disconformably overlain by the Saint Kilda Formation.|Laminated calcareous clays, intercalated with thin well-sorted sub-angular to well-rounded aeolian sands, commonly contains dolomite, high magnesian calcite and gypsum, and bivalves, foramanifera, turreted gastropods, sponge spicules, rare corals.|14-OCT-19
10825|Loxton Sand|2967|6|Mentioned|p35, 44|||See also references to Loxton Sands (p43, 45, 49). South Australia.|||||Marine.|
10825|Loxton Sand|10010|5|Briefly described|p12 Fig. 3|Late Pliocene|Early Pliocene|Misspelt - see Loxton Sands. Geological Province: Murray Basin.||||||13-AUG-07
10825|Loxton Sand|22773|5|Briefly described|Fig24.8p352,354||Pliocene|||||||
10825|Loxton Sand|22857|5|Briefly described|p339, p352 Fig. 24.8, p354|Late Pliocene|Late Pliocene|Marine sands. Heavy mineral sands containing rutile, zircon and ilmenite. Geological Province: Murray Basin.||||||
10825|Loxton Sand|23226|6|Mentioned|p901|||May overlap Pata Formation depending upon geographic location.  Of Murray Basin.||||||
10825|Loxton Sand|23482|5|Briefly described|p9|Tertiary|Tertiary|||||||
10825|Loxton Sand|23731|6|Mentioned|p29|Tertiary|Tertiary|||||||
10825|Loxton Sand|30928|6|Mentioned|Map legend|Pliocene|Pliocene|||||||
10825|Loxton Sand|32862|5|Briefly described|Table 3|||Lower Pliocene||||||
10825|Loxton Sand|33725|6|Mentioned|p9|||Small sinkholes.||||||
10825|Loxton Sand|33826|6|Mentioned|p42|||Strat. table||||||
10825|Loxton Sand|34418|6|Mentioned|p506|||Missing in Canopus Bore.||||||
10825|Loxton Sand|34757|6|Mentioned|p49|||||||||
10825|Loxton Sand|35071|6|Mentioned|Table 1|||||||||
10825|Loxton Sand|35174|6|Mentioned|p167|||||||||
10825|Loxton Sand|39322|6|Mentioned|Fig.3|||||||||
10825|Loxton Sand|40230|6|Mentioned|p6|||||||||
10825|Loxton Sand|41511|5|Briefly described|p19|||See also p20.||||||
10825|Loxton Sand|41537|6|Mentioned|Fig.2|||||||||
10825|Loxton Sand|41599|6|Mentioned|p192|||||||||
10825|Loxton Sand|42115|6|Mentioned|p7|||||||||
10825|Loxton Sand|42125|5|Briefly described|p137|||See also Fig.5||||||
10825|Loxton Sand|42126|6|Mentioned|p150|||||||||
10825|Loxton Sand|42127|5|Briefly described|p222|||||||||
10825|Loxton Sand|42130|6|Mentioned|Fig.3 P265|||||||||
10825|Loxton Sand|42132|6|Mentioned|Fig.5 P298|||||||||
10825|Loxton Sand|42134|4|Described|p339|||||||||
10825|Loxton Sand|42137|6|Mentioned|p370|||||||||
10825|Loxton Sand|42138|6|Mentioned|p392|||||||||
10825|Loxton Sand|43053|5|Briefly described|Map Legend|Pliocene|Pliocene|Fluviolacustrine and coastal, siliceous and clayey sand.||||||25-MAY-05
10825|Loxton Sand|43073|4|Described|p12,Table 3|||||||||
10825|Loxton Sand|43195|5|Briefly described|Map Legend||Early Pliocene|see also commentary on back of map.||||||
10825|Loxton Sand|43258|5|Briefly described|Map Legend||Pliocene|||||||
10825|Loxton Sand|43298|6|Mentioned|Map Legend||Pliocene|||||||
10825|Loxton Sand|43655|5|Briefly described|p40-846|||||||||
10825|Loxton Sand|44133|5|Briefly described|p161|Late Pliocene|Early Pliocene|Geological Province: Murray Basin. Overlies: Bookpurnong Formation conformably. See also Loxton Sands.||||||27-OCT-08
10825|Loxton Sand|49040|6|Mentioned|p12|||||||||
10825|Loxton Sand|60452|6|Mentioned|p37|Cenozoic|Cenozoic|Of Ludbrook (1957, 1961). Upper part then named Parilla Sand (Firman, 1965). Also called Diapur Sand in SA (Lawrence, 1966). Now refered to as Loxton-Parilla Sand to describe the unit across Victoria and South Australia.||||||19-NOV-08
10825|Loxton Sand|60540|5|Briefly described|p999,p1000 Fig.2,p1001, p1002 Fig.4, |Early Pliocene|Early Pliocene|Rogers et al. (1995). Shown as Loxton Sands in Firman (1972).||||Conformably overlies the Bookpurnong Formation. Partly correlative with Norwest Bend Formation in W Murray Basin.|Fluvial channel sands and contemporaneous shingled, regressive shoreline deposits and marine sediments.|06-FEB-18
10825|Loxton Sand|60785|5|Briefly described|p184 Fig.1, p196.  |Zanclean|Zanclean|South Australia. Has yielded fossil cetacean elements.|||||Poorly-sorted coarse sand containing pebbles.|
10825|Loxton Sand|60953|5|Briefly described|Map Legend|Pliocene|Pliocene|Marine to marginal marine.||||||
10825|Loxton Sand|61108|5|Briefly described|map legend|Pliocene|Pliocene|Arcuate ridges, partly inherited from coastal ridges in underlying marine to marginal marine Loxton Sand (not exposed).||||||
10825|Loxton Sand|61964|6|Mentioned|p139|||Regional correlative is Calivil Sand (Renmark Group). Geological Province: Murray Basin.||||||
10825|Loxton Sand|63124|6|Mentioned|p94||Pliocene|Geological Province: Gambier Basin.||||||
10825|Loxton Sand|64237|5|Briefly described|p18 Fig. 2, p19 Fig. 2b|Late Pliocene|Late Miocene|Included in the original stratigraphic scheme for the Murray Group and over- and underlying units of Lawrence (1961) and over/under-lying units of Lawrence (1961).||||||13-AUG-15
10825|Loxton Sand|64961|5|Briefly described|p269 Fig. 9|||Of Ludbrook (1961), Firman (1973)Pufahl et al (2004). Superseded by Loxton-Parilla Sand.||||||
10825|Loxton Sand|65715|5|Briefly described|p12, p15 Tb.8|Neogene|Neogene|Of Wunghnu Group. Senior synonym of Diapur Sandstone, Loxton-Parilla Sands and Parilla Sand in Victoria.||||||
10825|Loxton Sand|66002|5|Briefly described|p13 Tb.9, p18|Neogene|Neogene|Of Wunghnu Group. Defined by Ludbrook 1957. Marine. Difficult to distinguish from overlying aeolian Parilla Sand. Senior synonym of Diapur Sandstone and Dorodong Sands.||||||
10825|Loxton Sand|67179|4|Described|p579-85, p580 Fig.1b, p583 Fig.3, Fig.4|Early Pliocene|Late Miocene|Proposes to redefine Loxton Sand to incorporate all of the Loxton-Parilla Sands and the Parilla Sand(s). Diachronous ~10-7.2 Ma. Regressive arcuate strandplain sequence, 350km across, 600 strand-line ridges; due to marine regression in the Murray Basin. Previously the Loxton-Parilla Sands and Parilla Sands in VIC. Loxton Sand previously used for marine strata, but often not possible to separate from dune sands, so unit revised herein. Contains mineral sand deposits. Gamma spikes in downhole logs (due to monazite) show offsets (faulting) indicating Neogene tectonism. Depositional lithofacies: backshore dune, shoaling, breaker, surf and swash zones.|7.2 Ma (Sr isotope age of underlying sediments)||Divided into Kerang Sand Member, Tragowel Member, Wandella Sandstone Member in Kerang region.|Underlies the Shepparton Formation in east and Blanchetown Clay in NW, overlies the Bookpurnong Beds and the Renmark Group, interfingers with the Calivil Formation.|Incorporates shallow marine, beach dune, estuarine and fluvial sediments.|10-MAY-16
10825|Loxton Sand|67462|5|Briefly described|Map legend.|||Murray Basin.||||||
10825|Loxton Sand|68116|5|Briefly described|Maps 1-11, 14-17, 21-24, 29-30, 38-39.|Zanclean|Messinian|Also occurs in the Appendix.|||||Quartz sandstone: well sorted, fine to medium grained; well bedded; abundant lag horizons containing shelly fossils, pebble beds, rounded ironstone fragments; some heavy mineral concentrations; dissected or remobilised strand lines.|
10825|Loxton Sand|68194|6|Mentioned|p23|||SA name for Parilla Sand.||||||
10825|Loxton Sand|68548|5|Briefly described|p13|Pliocene|Pliocene|Early Pliocene age.||||Overlies Bookpurnong Formation. Grades into the Norwest Bend Formation to the west.|Comprises fluvial channel deposits and contemporaneous shallow marine sediments.|
10825|Loxton Sand|68715|6|Mentioned|p31 Fig.5|Pliocene|Miocene|Murray Basin. Late Miocene maximum age.||||||
10825|Loxton Sand|68716|5|Briefly described|p39-45|||Regionally extensive, unconfined or semi-confined aquifer. A source of lateral flow, saline groundwater discharges to the Murray River: c.one-half of the salt load entering in the Loxton reach.||||Overlain by the Blanchetown Clay. Underlain by the Bookpurnong Formation.||07-APR-17
10825|Loxton Sand|70718|4|Described|p24, p25, p28, p90-91, p104, p129|Pliocene|Late Miocene|Murray Basin. Formed in a marine to coastal environment and features aeolian, fluvial and lagoonal elements. Hosts economic heavy minerals in placer deposits that formed as a barrier system. Economic minerals include rutile, zircon, monazite, ilmenite and leucoxene. Deposition is linked to reactivated faults. Formerly the Loxton-Parilla Sands. From stratigraphic drill holes a thickness of 20-60m is interpreted a maximum thickness of 150m is interpreted from geophysics.||Wunghnu Group||Conformably overlies Bookpurnong beds. Disconformably overlies Renmark Group. Disconformably overlain by Blanchetown Clay. Overlain by Norwest Bend Formation. Interbedded with Calivil Formation.|High carbonate, yellow-brown, fine- to coarse-grained well-sorted sand; usually contains less than 15% clay with some pyrite.|02-JUN-19
10825|Loxton Sand|71593|4|Described|p53-p56, p60|Pliocene|Miocene|This unit is generally between 10-30m thick. Deposited in a high energy beach environment. Hosts heavy minerals. See also  p138-p139, p197-p198.||||Overlies the Bookpurnong Formation. Overlain by the Shepparton Formation. Equivalent to the Brighton Group.|Pebbly quartz sand that has been locally ferruginised.|
10825|Loxton Sand|72445|5|Briefly described|App.1, App.2; App 7 p7 Fig.4.|Pliocene|Pliocene|Shown as Loxton Sands in App.7. App.2 is a .csv format file. Identified in Stavely 01, 04, 05, 06, 08, 09, 10, 11, 14, 16. Variations to description in each hole. Locally gravelly Stavely 08, 09. Micaceous sand in Stavely 14.||Wunghnu Group.||Underlies Newer Volcanic Group, unconform.; Woorinen, Shepparton Fms, sharply. Overlies Olney Fm, gradational; Port Campbell Lst, Bookpurnong Fm, Geera Clay, sharply; Calivil Fm, sharply/gradational.|Silty sand to silty mud. Dominantly fine sand in Stavely01. Fine sand, locally muddy in Stavely02. Includes whitish yellow fine to coarse sand and mud. Some ferruginous concretions and organic staining in Stavely05. Includes silty and muddy sand.|
10825|Loxton Sand|73188|6|Mentioned|p320|Pliocene|Pliocene|Murray Basin.|||||Shallow marine calcareous sand, fluvial and coastal barrier sands.|
10825|Loxton Sand|73228|4|Described|p50-53, p55-60, p62|Early Pliocene|Late Miocene|Murray Basin. Shallow marine, beach dune, estuarine and fluvial sediments. Identified in Cooltong 1, Berri North 1, Nadda 1, and Loxton 1 drillholes. Interpreted as prograding beach strandplains and barrier islands. The beach sand contains [economic deposits of] heavy minerals, including ilmenite, zircon, rutile and tourmaline.||||Conformably underlain by and possible equivalent to Bookpurnong Formation. Underlain by Parilla Sand. Overlain by Blanchetown Clay and Molineaux Sand.|Glauconitic, micaceous and shelly fine sand, overlain by planar and cross-bedded fine to coarse-grained sand and fine gravel, and planar bedded, calcareous, micaceous, medium- to coarse-grained sandstone with abundant shell debris.|
10825|Loxton Sand|73229|5|Briefly described|p66-67, p70, p72, p74|Early Pliocene|Late Miocene|Murray Basin. [Analysed using pXRF; see article]. Shallow marine, beach, aeolian, lacustrine and fluvial.|||||Includes sand, glauconitic, micaceous, and shelly gravel; coarse-grained sand and fine gravel, and calcareous micaceous, medium- to coarse-grained sandstone.|
10825|Loxton Sand|73253|6|Mentioned|p13-14, p16|Late Miocene|Late Miocene|Murray Basin. Includes heavy mineral deposits. Preserved as paleostrandlines. Samples collected for heavy mineral provenance; interpreted to represent fluvial inputs from as far as Queensland but dominantly from the southeast via the ancestral Murray River (dominantly) and Darling River.||||||
10890|Lyndhurst Formation|22510|5|Briefly described|p38, Table1p37|||Age: Sturtian||||||
10890|Lyndhurst Formation|22772|5|Briefly described|Table13.1|Cryogenian|Cryogenian|||||||
10890|Lyndhurst Formation|22857|5|Briefly described|Tb. 13.1 (insert p70-71)|Sturtian|Sturtian|Of the Yudnamutana Subgroup (Umberatana Group).||||||
10890|Lyndhurst Formation|23394|5|Briefly described|Map legend|Proterozoic|Proterozoic|||||||
10890|Lyndhurst Formation|23411|6|Mentioned|Map Legend|||||||||
10890|Lyndhurst Formation|23818|4|Described|p64 Fig.22|Neoproterozoic|Neoproterozoic|Uppermost unit of the Yudnamutana Sub-Group. Underlying unit: Bolla Bollana Formation. Max. thickness: >4 000 ft.||||||
10890|Lyndhurst Formation|24176|4|Described|p11, p25 Tb. 1|Adelaidean|Adelaidean|Of Yudnamutana Sub-Group (Umberatana Group).  Grey-blue shale, minor quartzite boulder beds.  Overlies Bolla Bollana Formation.  Age is Sturtian.  Max. thickness: 1280m.  Geological Province: Mount Painter Province.||||||
10890|Lyndhurst Formation|24546|5|Briefly described|p2 - 3 Fig.2|Neoproterozoic|Neoproterozoic|Of Umberatana Group. Overlies Bolla Bollana Formation. Geological Province: Adelaide Fold Belt.||||||16-JAN-08
10890|Lyndhurst Formation|30176|6|Mentioned|Map legend|Precambrian|Precambrian|Sturtian||||||
10890|Lyndhurst Formation|30177|5|Briefly described|p75|||||||||
10890|Lyndhurst Formation|30178|6|Mentioned|p19|||||||||
10890|Lyndhurst Formation|30801|6|Mentioned|p5|||Table P5-6. Yudnamutana Sub-Group||||||
10890|Lyndhurst Formation|30807|6|Mentioned|p103|||Suggested map symbol||||||
10890|Lyndhurst Formation|32364|6|Mentioned|p17|||||||||
10890|Lyndhurst Formation|32724|6|Mentioned|Fig.1|||Correlation||||||
10890|Lyndhurst Formation|33474|6|Mentioned|Fig.2|||||||||
10890|Lyndhurst Formation|34535|6|Mentioned|p65|||See Fig.22.  Yudnamutana Subgroup||||||
10890|Lyndhurst Formation|35255|6|Mentioned|Fig.7|||||||||
10890|Lyndhurst Formation|35264|6|Mentioned|p13|||||||||
10890|Lyndhurst Formation|36137|6|Mentioned|p11|||||||||
10890|Lyndhurst Formation|36253|6|Mentioned|Fig.3-2|||||||||
10890|Lyndhurst Formation|36733|6|Mentioned|Table 5|||||||||
10890|Lyndhurst Formation|37932|5|Briefly described|p539|||||||||
10890|Lyndhurst Formation|38157|6|Mentioned|Table IV|||||||||
10890|Lyndhurst Formation|39344|6|Mentioned|Map legend|Precambrian|Precambrian|Sturtian||||||
10890|Lyndhurst Formation|40294|6|Mentioned|p41|||||||||
10890|Lyndhurst Formation|41364|6|Mentioned|p152|||||||||
10890|Lyndhurst Formation|41405|3|Fully described|p134|||||||||
10890|Lyndhurst Formation|41647|6|Mentioned|p839|||||||||
10890|Lyndhurst Formation|41770|6|Mentioned|p238|||||||||
10890|Lyndhurst Formation|42222|5|Briefly described|p16|||||||||
10890|Lyndhurst Formation|43052|5|Briefly described|p183,Table 6.1|||of Yudnamutana Subgroup||||||
10890|Lyndhurst Formation|62903|6|Mentioned|p729|||Adelaide Rift Complex.||Yudnamutana Subgroup||||
10890|Lyndhurst Formation|67180|6|Mentioned|p602 Fig.2|Cryogenian|Cryogenian|Sturtian age, of Northern Flinders Ranges (Preiss et al. 1998).||Unit in Umberatana Group||Overlies the Bolla Bollana Tillite.||
10890|Lyndhurst Formation|67979|5|Briefly described|p529, p531 Fig.2, p535 Fig.6, p541|Sturtian||In Northern Flinders Ranges. Glacials.||Yudnamutana Subgroup||Angular unconformity with overlying Serle Conglomerate Member (Tapley Hill Formation) at Tindelpina Hut section (Young and Gostin 1989).|Dropstone-bearing shales, glacigenic.|22-SEP-14
10890|Lyndhurst Formation|69019|6|Mentioned|p41.|Neoproterozoic|Neoproterozoic|Not in this map area.||Unit in Yudnamutana Subgroup.||Is equivalent to Wilyerpa Formation.||
10890|Lyndhurst Formation|69023|6|Mentioned|p64|Neoproterozoic|Neoproterozoic|||Unit in Yudnamutana Subgroup.||||
10890|Lyndhurst Formation|70384|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Adelaide Geosyncline. Age shown more specifically as Sturtian [Cryogenian].||Yudnamutana Subgroup.|||Blue-grey siltstone with occasional lonestones and quartzite interbeds.|21-JAN-19
10890|Lyndhurst Formation|71237|2|Defined|p7, 8, 10, 18|||||||||
10919|MacDonnell Member|32898|6|Mentioned|Table 2-1|||Paaratte Fm.||||||
10931|Macclesfield Marble|30377|6|Mentioned|p200|||||||||
10931|Macclesfield Marble|34615|6|Mentioned|p7|||Shown on Figure.||||||
10931|Macclesfield Marble|42222|6|Mentioned|Table 1 P4|||||||||
10931|Macclesfield Marble|42268|5|Briefly described|p330|||||||||
10931|Macclesfield Marble|44133|6|Mentioned|p10 |||||||||
10952|Mackunda Formation|12597|5|Briefly described|p492 Tb.1, p500|Cenomanian|Cenomanian|Eromanga Basin. 60m thick.|||||Marginal marine sequence; labile sandstone, siltstone and mudstone, calcareous in part, containing bivalves, ammonites, belemnites, polyzoans and sharks' teeth.|
10952|Mackunda Formation|13497|5|Briefly described|p115 fig 6.33, p146, p149-p154, |Early Cretaceous|Early Cretaceous|Eromanga Basin. Mis-spelt as the Macunda Formation on p146.||Marree Subgroup||Overlies the Allaru Mudstone and the Oodnadatta Formation. Overlain by the Winton Formation.||
10952|Mackunda Formation|13516|6|Mentioned|p167 fig 10, p169 fig 11, p171 fig 12|Late Cretaceous|Late Cretaceous|In Eromanga Basin.||||||
10952|Mackunda Formation|22857|5|Briefly described|p296-7 Tb.22.1|Cenomanian|Albian|Of the Rolling Downs Group. Geological Province: Eromanga Basin.||||||
10952|Mackunda Formation|22865|5|Briefly described|Table22.1p296-7|Cenomanian|Albian|||||||
10952|Mackunda Formation|22883|5|Briefly described|Fig2 P30||Late Cretaceous|Overlying unit is Winton Formation, underlying unit is Allura Mudstone||||||
10952|Mackunda Formation|22912|5|Briefly described|33|||Geol province Eromanga Basin||||||
10952|Mackunda Formation|23056|6|Mentioned|12 table 2|||||||||
10952|Mackunda Formation|23154|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|Geological Province - Eromanga Basin. Of the Neales River Group.||||||20-FEB-07
10952|Mackunda Formation|23155|4|Described|p33|Early Cretaceous|Early Cretaceous|Determination of the spore-pollen assemblage indicate an Early Cretaceous (Albian) age. The unit conformably overlies both the Allaru Mudstone and Oodnadatta Formation on STRZELECKI.||||||11-NOV-13
10952|Mackunda Formation|23183|6|Mentioned|p223||Albian|||||||
10952|Mackunda Formation|23188|6|Mentioned|p283,287||Albian|||||||
10952|Mackunda Formation|23375|4|Described|Fig2 p265|Cenomanian|Albian|In the Eromanga Basin.||||||31-OCT-06
10952|Mackunda Formation|23425|5|Briefly described|Plate 10.2|||In the Eromanga Basin Province.||||||20-FEB-07
10952|Mackunda Formation|23430|4|Described|p524 Table 14.7|||Eromanga Basin Province. Maximum thickness <275 m.||||||
10952|Mackunda Formation|23818|6|Mentioned|p141 Fig.65|||Geological Province: Great Artesian Basin. Of the Manuka Sub-Group.||||||
10952|Mackunda Formation|23883|5|Briefly described|p129 Fig. 11.2|Cretaceous|Cretaceous|Of Rolling Downs Group. Geological Province: Great Australian Superbasin.||||||
10952|Mackunda Formation|23911|5|Briefly described|p97 Fig. 11|Cretaceous|Cretaceous|Geological Province: Eromanga Basin.  Of the Rolling Downs Group.||||||
10952|Mackunda Formation|23982|5|Briefly described|p35 Fig.7|Cretaceous|Cretaceous|Of Rolling Downs Group. Geological Province: Great Artesian Basin.||||||
10952|Mackunda Formation|24092|5|Briefly described|p5|Cretaceous|Cretaceous|Geological Province: Great Artesian Basin.||||||
10952|Mackunda Formation|24175|3|Fully described|p28, p17 Fig. 3|Cenomanian|Albian|Overlain by Winton Formation; overlies Allaru Mudstone. Max. thickness: 57m. Geological Province: Eromanga Basin.||||||11-NOV-13
10952|Mackunda Formation|24204|5|Briefly described|p263 Fig.4, p267|Early Cretaceous|Early Cretaceous|Geological Province: Eromanga Basin.||||||
10952|Mackunda Formation|24210|5|Briefly described|p133 Fig. 2|Late Cretaceous|Early Cretaceous|Geological Province: Eromanga Basin.||||||
10952|Mackunda Formation|24251|5|Briefly described|p234 Fig.1, p245|Albian|Albian|Underlain by Allaru Formation. Geological Province: Eromanga Basin||||||20-FEB-07
10952|Mackunda Formation|24321|5|Briefly described|Map legend|Cenomanian|Albian|Of the Neales River Group.||||||31-OCT-06
10952|Mackunda Formation|29591|6|Mentioned|p71|||||||||
10952|Mackunda Formation|30019|6|Mentioned|p2|||Upper Albian||||||
10952|Mackunda Formation|30020|6|Mentioned|p35|||||||||
10952|Mackunda Formation|30103|5|Briefly described|p9|||Unit of Rolling Downs Group. Table 3 on p9.||||||31-OCT-06
10952|Mackunda Formation|30104|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
10952|Mackunda Formation|30691|4|Described|p17|||See also p22,Table 4,6. Lower-Upper Cretaceous.||||||31-OCT-06
10952|Mackunda Formation|30804|6|Mentioned|p10|||||||||
10952|Mackunda Formation|30853|5|Briefly described|Table 3|||Albian age||||||
10952|Mackunda Formation|30854|4|Described|Table 4|||Albian||||||
10952|Mackunda Formation|30855|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|Rolling Downs Group||||||
10952|Mackunda Formation|30856|6|Mentioned|p10|||||||||
10952|Mackunda Formation|31098|6|Mentioned|p10|||||||||
10952|Mackunda Formation|31144|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
10952|Mackunda Formation|31145|5|Briefly described|Table 1|||Lower Cretaceous||||||
10952|Mackunda Formation|31208|6|Mentioned|Fig. 7|||||||||
10952|Mackunda Formation|31425|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
10952|Mackunda Formation|31430|5|Briefly described|Table 1|||L.Cretaceous||||||
10952|Mackunda Formation|31431|5|Briefly described|Table 3|||Lower Cretaceous.||||||
10952|Mackunda Formation|31432|4|Described|Table 1|||L.Cretaceous||||||
10952|Mackunda Formation|31434|6|Mentioned|p8|||||||||
10952|Mackunda Formation|31436|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
10952|Mackunda Formation|31438|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
10952|Mackunda Formation|31441|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
10952|Mackunda Formation|31553|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
10952|Mackunda Formation|31572|4|Described|Fig. 1|||L.Cretaceous||||||
10952|Mackunda Formation|32277|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower Cretaceous - Upper Cretaceous.||||||
10952|Mackunda Formation|32314|6|Mentioned|Fig. 4|||||||||
10952|Mackunda Formation|32395|6|Mentioned|p7|||Correlation||||||
10952|Mackunda Formation|32396|6|Mentioned|p9|||Correlated with Normanton Fm.||||||
10952|Mackunda Formation|32553|4|Described|p38|||||||||
10952|Mackunda Formation|32796|6|Mentioned|p303|||||||||
10952|Mackunda Formation|33016|6|Mentioned|p1|||Table on P1||||||
10952|Mackunda Formation|33067|4|Described|Table 1|Early Cretaceous|Early Cretaceous|Of the Rolling Downs Group.||||||07-JUL-04
10952|Mackunda Formation|33069|4|Described|p7|||L.-U.Cret.||||||
10952|Mackunda Formation|33073|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
10952|Mackunda Formation|33075|6|Mentioned|Table 1|||||||||
10952|Mackunda Formation|33078|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
10952|Mackunda Formation|33079|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
10952|Mackunda Formation|33082|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
10952|Mackunda Formation|33083|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
10952|Mackunda Formation|33086|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower to Upper Cretaceous||||||
10952|Mackunda Formation|33087|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
10952|Mackunda Formation|33088|4|Described|Table 3|||Of the Rolling Downs Group.||||||20-FEB-07
10952|Mackunda Formation|33089|4|Described|Table 2|||L.Cret.||||||
10952|Mackunda Formation|33165|6|Mentioned|Chart|||Correlation chart only||||||
10952|Mackunda Formation|33176|6|Mentioned|p171|||||||||
10952|Mackunda Formation|33182|6|Mentioned|p200|||L.Cret. See also Table 1||||||
10952|Mackunda Formation|33368|6|Mentioned|p25|||Strat.table.||||||
10952|Mackunda Formation|33372|6|Mentioned|Table 1|||||||||
10952|Mackunda Formation|33414|6|Mentioned|p211|||||||||
10952|Mackunda Formation|33561|6|Mentioned|p102|||||||||
10952|Mackunda Formation|33638|5|Briefly described|Table 1|||||||||
10952|Mackunda Formation|33639|5|Briefly described|Table 2|||L.Cret.||||||
10952|Mackunda Formation|33640|4|Described|Table 2|||L.Cret.||||||
10952|Mackunda Formation|33642|6|Mentioned|p144-5,147-8,Tb.1,|||Refers Vine & Day (1965). Figs. 1 & 2.||||||
10952|Mackunda Formation|33643|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
10952|Mackunda Formation|33647|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
10952|Mackunda Formation|33648|6|Mentioned|p19|||Stratigraphy.||||||
10952|Mackunda Formation|33825|6|Mentioned|p10|||Correlation table||||||
10952|Mackunda Formation|33832|5|Briefly described|p11|||Stratigraphy and correlation.||||||31-OCT-06
10952|Mackunda Formation|33964|4|Described|p6|||||||||
10952|Mackunda Formation|34065|4|Described|p6|||L.Cret.||||||
10952|Mackunda Formation|34091|5|Briefly described|Table 1|||L.Cret||||||
10952|Mackunda Formation|34174|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower - Upper Cretaceous||||||
10952|Mackunda Formation|34217|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
10952|Mackunda Formation|34218|4|Described|Table 1|||Lower Cretaceous. See also Table 2.||||||
10952|Mackunda Formation|34356|6|Mentioned|p21|||Albian.||||||
10952|Mackunda Formation|34485|4|Described|Table 1|||Lower - Upper Cretaceous||||||
10952|Mackunda Formation|34486|4|Described|Table 1|||Lower - Upper Cretaceous||||||
10952|Mackunda Formation|34487|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
10952|Mackunda Formation|34611|6|Mentioned|Fig.65|||Correlation chart||||||
10952|Mackunda Formation|34619|3|Fully described|p.160. Pl.22||Adelaidean|||||||
10952|Mackunda Formation|35139|4|Described|Table.2|||||||||
10952|Mackunda Formation|35239|6|Mentioned|Fig.4|||||||||
10952|Mackunda Formation|35560|6|Mentioned|Fig.3|||||||||
10952|Mackunda Formation|35793|6|Mentioned|Fig.3|||||||||
10952|Mackunda Formation|35811|5|Briefly described|Table 3|||||||||
10952|Mackunda Formation|35855|6|Mentioned|Fig.2|||Early Cretaceous lithostratigraphy.||||||
10952|Mackunda Formation|36229|6|Mentioned|Map legend|Mesozoic|Mesozoic|||||||
10952|Mackunda Formation|36243|6|Mentioned|Table 6A|||||||||
10952|Mackunda Formation|36552|6|Mentioned|Fig.25|||||||||
10952|Mackunda Formation|36571|6|Mentioned|p101|||See also Table 4.||||||
10952|Mackunda Formation|37263|6|Mentioned|p319|||||||||
10952|Mackunda Formation|37451|6|Mentioned|Table 2|||||||||
10952|Mackunda Formation|37608|3|Fully described|Table 1|||||||||
10952|Mackunda Formation|38226|6|Mentioned|Table 1|||||||||
10952|Mackunda Formation|38373|6|Mentioned|p621|||||||||
10952|Mackunda Formation|38779|6|Mentioned|p4|||||||||
10952|Mackunda Formation|38814|6|Mentioned|Table 1|||||||||
10952|Mackunda Formation|39070|4|Described|p366|||||||||
10952|Mackunda Formation|39211|5|Briefly described|Fig.3|||See also Figs 4,7,11,13 etc. Correlation||||||
10952|Mackunda Formation|39445|5|Briefly described|Table 11|||||||||
10952|Mackunda Formation|39478|6|Mentioned|Table 1|||||||||
10952|Mackunda Formation|39846|6|Mentioned|Fig.2|||||||||
10952|Mackunda Formation|39847|5|Briefly described|p40|||||||||
10952|Mackunda Formation|39943|6|Mentioned|Table 8A|||||||||
10952|Mackunda Formation|40121|6|Mentioned|Table 1|||||||||
10952|Mackunda Formation|40199|6|Mentioned|Fig.2|||||||||
10952|Mackunda Formation|40220|6|Mentioned|Fig.2|||||||||
10952|Mackunda Formation|40249|6|Mentioned|p41|||||||||
10952|Mackunda Formation|40675|6|Mentioned|Table 8A|||||||||
10952|Mackunda Formation|40681|6|Mentioned|Fig.2|||||||||
10952|Mackunda Formation|40687|3|Fully described|p419|||||||||
10952|Mackunda Formation|40801|6|Mentioned|p42|||||||||
10952|Mackunda Formation|40910|6|Mentioned|p17|||||||||
10952|Mackunda Formation|40926|6|Mentioned|p19|||||||||
10952|Mackunda Formation|41060|6|Mentioned|p2|||Generalized stratigraphy||||||
10952|Mackunda Formation|41062|6|Mentioned|Fig.5|||||||||
10952|Mackunda Formation|41063|6|Mentioned|p40|||||||||
10952|Mackunda Formation|41064|6|Mentioned|p62|||||||||
10952|Mackunda Formation|41084|5|Briefly described|Fig.2|||||||||
10952|Mackunda Formation|41085|6|Mentioned|p89|||||||||
10952|Mackunda Formation|41086|3|Fully described|p98, Fig.3|||||||||
10952|Mackunda Formation|41088|6|Mentioned|Fig.2|||||||||
10952|Mackunda Formation|41097|6|Mentioned|Table 1|||||||||
10952|Mackunda Formation|41099|6|Mentioned|Fig.9|||||||||
10952|Mackunda Formation|41165|5|Briefly described|p363|||Mention Fig.15||||||
10952|Mackunda Formation|41176|6|Mentioned|Table 2|||||||||
10952|Mackunda Formation|41177|6|Mentioned|Fig.2|||||||||
10952|Mackunda Formation|41182|5|Briefly described|Fig.2|||||||||
10952|Mackunda Formation|41183|6|Mentioned|Fig.3 p308|||||||||
10952|Mackunda Formation|41187|6|Mentioned|Fig.2|||||||||
10952|Mackunda Formation|41198|6|Mentioned|Table 1|||||||||
10952|Mackunda Formation|41214|6|Mentioned|Fig.3|||||||||
10952|Mackunda Formation|41216|6|Mentioned|Fig.18|||||||||
10952|Mackunda Formation|41266|6|Mentioned|Fig.3|||||||||
10952|Mackunda Formation|41523|3|Fully described|p282|||See also p277.||||||31-OCT-06
10952|Mackunda Formation|41707|6|Mentioned|Fig.8|||||||||
10952|Mackunda Formation|41724|6|Mentioned|p383|||||||||
10952|Mackunda Formation|41950|5|Briefly described|Fig.2 P3|||||||||
10952|Mackunda Formation|42061|4|Described|Fig,11 P159|||||||||
10952|Mackunda Formation|42067|4|Described|Appendix 2|||See also Fig.2 p309.||||||31-OCT-06
10952|Mackunda Formation|42071|6|Mentioned|p117|||||||||
10952|Mackunda Formation|42084|6|Mentioned|Fig.3 P356|||||||||
10952|Mackunda Formation|42085|6|Mentioned|Fig.2 P374|||||||||
10952|Mackunda Formation|42395|5|Briefly described|Fig.13 P83|||||||||
10952|Mackunda Formation|42397|6|Mentioned|Fig.2 P3|||||||||
10952|Mackunda Formation|42429|6|Mentioned|Figs.6 & 9 P156|||||||||
10952|Mackunda Formation|42446|4|Described|p14|||||||||
10952|Mackunda Formation|42447|6|Mentioned|Fig. 1|||||||||
10952|Mackunda Formation|42477|5|Briefly described|p166|||||||||
10952|Mackunda Formation|42496|5|Briefly described|p136, Fig.3 p132|||||||||
10952|Mackunda Formation|42520|5|Briefly described|p6|||||||||
10952|Mackunda Formation|42673|5|Briefly described|Fig.2, P184|||||||||
10952|Mackunda Formation|42746|5|Briefly described|p12|||See also Fig.6||||||
10952|Mackunda Formation|42749|6|Mentioned|Fig.2 P27|||||||||
10952|Mackunda Formation|42999|5|Briefly described|Table 2,p90||Late Cretaceous|||||||
10952|Mackunda Formation|43002|5|Briefly described|Fig.2,p135|||||||||
10952|Mackunda Formation|43004|5|Briefly described|Table 1,p179|||||||||
10952|Mackunda Formation|43053|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Marginal marine sandstone and siltstone. Includes Mount Howie Sandstone.||||||25-MAY-05
10952|Mackunda Formation|43105|6|Mentioned|p15|||||||||
10952|Mackunda Formation|43114|5|Briefly described|p16|||||||||
10952|Mackunda Formation|43122|5|Briefly described|Fig.2.|||||||||
10952|Mackunda Formation|43258|5|Briefly described|Map Legend||Cretaceous|||||||
10952|Mackunda Formation|43298|5|Briefly described|Map Legend||Cretaceous|||||||
10952|Mackunda Formation|43591|6|Mentioned|p40|||||||||
10952|Mackunda Formation|43628|6|Mentioned|Fig.3|Early Cretaceous|Early Cretaceous|||||||
10952|Mackunda Formation|44016|14|Not recorded|Map Legend||Early Cretaceous|||||||
10952|Mackunda Formation|44017|14|Not recorded|Map Legend|||||||||
10952|Mackunda Formation|44018|14|Not recorded|Map Legend||Early Cretaceous|||||||
10952|Mackunda Formation|44019|14|Not recorded|Map Legend||Early Cretaceous|||||||
10952|Mackunda Formation|44020|14|Not recorded|p10,Tb.1,2||Early Cretaceous|Of roling Dwons Grouop.||||||
10952|Mackunda Formation|44031|14|Not recorded|p3,5,8,9||Cretaceous|||||||
10952|Mackunda Formation|44033|14|Not recorded|map,p4,5,8,9||Cretaceous|||||||
10952|Mackunda Formation|44034|4|Described|Tb.1,p2,4-6,9,10|||||||||
10952|Mackunda Formation|44042|14|Not recorded|Map Legend||Early Cretaceous|||||||
10952|Mackunda Formation|44067|14|Not recorded|Map Legend||Early Cretaceous|||||||
10952|Mackunda Formation|44082|6|Mentioned|p6,12,26,28,Tb.p34||Albian|Mentioned with respect to Qld Cretaceous fossils which are either of stratigraphic significance or are illustrative of the occurrence of a particular group.||||||
10952|Mackunda Formation|44089|4|Described|Tb.1,p3,4,8,9,map||Early Cretaceous|||||||
10952|Mackunda Formation|44091|14|Not recorded|p60|||||||||
10952|Mackunda Formation|44133|4|Described|p122-123, 104 Fig. 9.11|Early Cenomanian|Late Albian|Geological Province: Eromanga Basin. Conformably overlies Oodnadatta Formation and Allaru Mudstone. Contains sediments from the now superseded Mount Alexander Sandstone Member and Blanchewater Formation.||||||
10952|Mackunda Formation|44361|14|Not recorded|Map Legend||Early Cretaceous|||||||
10952|Mackunda Formation|44362|4|Described|p12,Tb.1||Early Cretaceous|||||||
10952|Mackunda Formation|44374|14|Not recorded|p12||Cretaceous|early Late Albian sandstone,siltstone indicating shoaling of seas throughout Eromanga Basin.||||||
10952|Mackunda Formation|44376|14|Not recorded|p6|||||||||
10952|Mackunda Formation|44410|14|Not recorded|Map Legend||Early Cretaceous|||||||
10952|Mackunda Formation|44414|14|Not recorded|p110-112|||Sandstone, mudstone characterised by marine fossils overlain by Winton Formation.||||||
10952|Mackunda Formation|44417|2|Defined|p416,419-420|||Formerly called Mackunda Beds. Overlies Wilgunya Formation. Albian fossils. Unit of Rolling Downs Group.||||||31-OCT-06
10952|Mackunda Formation|44418|14|Not recorded|Map Legend||Early Cretaceous|||||||
10952|Mackunda Formation|44573|14|Not recorded|p98||Cretaceous|||||||
10952|Mackunda Formation|44807|14|Not recorded|unknown (p1-16)|||Allaru Mudstone, correlated with Normanton Formation.||||||
10952|Mackunda Formation|44915|14|Not recorded|p18|||Ref. to Vine and Day 1965. Comparable to lower part of Blanchewater Formation in South Australia.||||||
10952|Mackunda Formation|44920|14|Not recorded|Map Legend,Sheet 4||Cretaceous|||||||
10952|Mackunda Formation|45052|5|Briefly described|p134|||Mesozoic||||||
10952|Mackunda Formation|45103|6|Mentioned|p8|||||||||
10952|Mackunda Formation|45110|6|Mentioned|p147|||See also Table 18.||||||
10952|Mackunda Formation|45168|6|Mentioned|p6|||||||||
10952|Mackunda Formation|46791|5|Briefly described|p48|||||||||
10952|Mackunda Formation|46937|5|Briefly described|Fig.10|||See also Table 1.||||||
10952|Mackunda Formation|48920|3|Fully described|p62|||||||||
10952|Mackunda Formation|49010|6|Mentioned|Fig.4|||Eromanga Basin||||||
10952|Mackunda Formation|49011|6|Mentioned|Fig.3|||Eromanga Basin||||||
10952|Mackunda Formation|50100|5|Briefly described|p23|Cretaceous|Cretaceous|Of the Rolling Downs Group.  Geological Province: Eromanga Basin.||||||
10952|Mackunda Formation|60331|5|Briefly described|p34 Fig.3|Albian|Albian|Overlies Allaru Mudstone. Overlain by Winton Formation. Geological Province: Eromanga Basin.||||||
10952|Mackunda Formation|60717|5|Briefly described|p40 Fig. 2|Early Cretaceous|Early Cretaceous|Overlies Allaru Mudstone and Oodnadatta Formation, with which it also interfingers laterally. Overlain by Winton Formation. Geological Province: Eromanga Basin.||||||31-JAN-08
10952|Mackunda Formation|60953|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Marginal marine sandstone and siltstone.||||||
10952|Mackunda Formation|61312|5|Briefly described|p64, p79 Table E2|Cretaceous|Cretaceous|Of the Rolling Downs Group. Siltstone, sandstone, minor shale. Geological Province: Eromanga Basin (absent in NSW).||||||
10952|Mackunda Formation|61611|6|Mentioned|p265 Fig. 3|Early Cretaceous|Early Cretaceous|Geological Province: Eromanga Basin.||||||13-MAR-09
10952|Mackunda Formation|61613|6|Mentioned|p282 Fig. 2|Late Cretaceous|Late Cretaceous|Geological Province: Eromanga Basin.||||||07-FEB-11
10952|Mackunda Formation|61614|6|Mentioned|p290 Fig. 2|Late Cretaceous|Early Cretaceous|Geological Province: Eromanga Basin.||||||17-MAR-09
10952|Mackunda Formation|61615|6|Mentioned|p302 Fig. 2|Late Cretaceous|Early Cretaceous|Geological Province: Eromanga Basin.||||||07-FEB-11
10952|Mackunda Formation|62028|5|Briefly described|p10 Fig. 1|||||||||
10952|Mackunda Formation|62029|5|Briefly described|p15 Fig. 4|Cretaceous|Cretaceous|||||||
10952|Mackunda Formation|62046|5|Briefly described|p125 Fig. 2|Cretaceous|Cretaceous|Geological Province: Cooper-Eromanga Basins.||||||14-APR-08
10952|Mackunda Formation|62376|5|Briefly described|p84|Early Cretaceous|Early Cretaceous|Geological Province: Pedirka Basin.||||||09-FEB-10
10952|Mackunda Formation|62537|6|Mentioned|p191 Fig.2. |Late Cretaceous|Late Cretaceous|Eromanga Basin.||||Overlies Oodnadatta and Allaru Formations. Is overlain by Winton Formation.||
10952|Mackunda Formation|62730|5|Briefly described|p352 Fig. 1|Late Cretaceous|Late Cretaceous|Geological Province: Eromanga Basin.||||||21-APR-08
10952|Mackunda Formation|63979|2|Defined|p53, Fig. 44|Cenomanian|Albian|Previously Mackunda Beds (Vine 1964). Of Manuka Subgroup (Rolling Downs Gp). Conformable on Allaru Mudstone. Conformable below Winton Fm. Max. thick: 150m. Interbedded sandstone, siltstone and mudstone and lesser mudclast intraformational conglomerate.||||||07-FEB-11
10952|Mackunda Formation|64048|6|Mentioned|p64 Tb. 2, p72|||Geological Province: Eromanga Basin.||||||07-FEB-11
10952|Mackunda Formation|64197|6|Mentioned|p625 Fig.1c, p630 Figs.6,7|Cretaceous|Cretaceous|Eromanga Basin.||||Overlies Allaru Mudstone (Marree Subgroup); is overlain by Winton Formation.||10-DEC-15
10952|Mackunda Formation|64665|6|Mentioned|p62.|Cretaceous|Cretaceous|Eromanga Basin.||||||
10952|Mackunda Formation|65238|5|Briefly described|p7 Fig. 8|Early Cretaceous|Early Cretaceous|Geological province: Eromanga Basin. Transgressive marine deposits.||||||
10952|Mackunda Formation|65376|5|Briefly described|p9 Fig.1.2. |Cretaceous|Cretaceous||||||Marginal marine to fluvial mudstone and siltstone.|
10952|Mackunda Formation|65385|5|Briefly described|pS134 Fig.7|Late Cretaceous|Early Cretaceous|Of Eromanga Basin. Overlies Allaru Mudstone and Oodnadatta Formation. Overlain by Winton Formation.||||||08-MAR-12
10952|Mackunda Formation|65489|5|Briefly described|p49, p55, p58, p61, p96, p155|Early Cretaceous|Early Cretaceous|Eromanga Basin. 200m thick. Regional seal.||||Overlies Allaru Mudstone. Is overlain by Winton Formation.||
10952|Mackunda Formation|65925|5|Briefly described|Appendix 2.||||||||Calcareous sandstone; siltstone; shale.|
10952|Mackunda Formation|66518|6|Mentioned|p19 Fig.4.|Cretaceous|Cretaceous|Eromanga Basin.||||Overlies Oodnadatta Formation.||06-FEB-14
10952|Mackunda Formation|66529|6|Mentioned|p12 Fig.5, p16  |||||Unit in Rolling Downs Group.||Overlies Oodnadatta Formation and Allaru Mudstone. Is overlain by Winton Formation.||
10952|Mackunda Formation|66623|6|Mentioned|pp264-265.|||Partly equivalent to Allaru Mudstone in Koonenberry Belt, NSW.||||Overlies Allaru Mudstone.||
10952|Mackunda Formation|67323|5|Briefly described|p87, p92, p93 Fig.12.3, p95 Fig.12.5|Cretaceous|Cretaceous|See also GIS attrib tbl, Solid Geology Map. Eromanga/Carpentaria Basins.||||Overlies Allaru Mudstone. Is overlain by Winton Formation.|Feldspathic sandstone, siltstone.|
10952|Mackunda Formation|67402|4|Described|p26 tbl RRM4|Cenomanian|Albian|Eromanga Basin. Deposited in shallow marine or paralic environments. Maximum thickness of 100m. Estimated porosity of 10-25% with unknown permeability. See also p108, p109, p115 tbl ERO2.||||Overlies the Allaru Mudstone. Overlain by the Winton Formation.|Very fine to fine-grained sandstone, with laminations of siltstone and mudstone and lesser mud-clast intraformational conglomerate.|
10952|Mackunda Formation|67784|5|Briefly described|p25-26, p28-32|Albian|Albian|Northern Eromanga Basin. 90-275m thick.||||Overlies Allaru Formation, overlain by Winton Formation|Contains labeceratid ammonites.|08-FEB-18
10952|Mackunda Formation|68068|5|Briefly described|Map legend|Albian|Albian|Eromanga Basin. Marginal marine to paralic; a marine regression. Fossiliferous: molluscs, forams, wood, diverse microflora, fish and vertebrates.||Unit in Neales River Group.||Conformably overlies Oodnadatta Formation. Is overlain conformably by Winton Formation.|Bimodal cross-bedded, yellow-brown fine to medium sand interbedded with greenish to grey silt and silty clay; then pale grey-green, interbedded, cross-bedded, glauconitic, sand-silt-shale and calcareous shales, mud and clay intraclasts common.|
10952|Mackunda Formation|68131|5|Briefly described|p2 Fig.1|Cretaceous|Cretaceous|Marginal marine to fluvial sediments. Mapped with Mackunda Formation as one unit.|||||Mudstone and siltstone.|
10952|Mackunda Formation|68206|6|Mentioned|p31-33|Albian|Albian|NE Eromanga Basin.||||Overlies Allaru Formation.||
10952|Mackunda Formation|68279|6|Mentioned|p18|||Galilee Basin stratigraphic cross-sections, and mineralogy tables.||||||
10952|Mackunda Formation|68553|6|Mentioned|Map legend; schematic diagram.|Cretaceous|Cretaceous|Eromanga and Carpentaria Basins.||Unit in Rolling Downs Group.||Conformably overlies Allaru Mudstone. Is overlain conformably by Winton Formation.||
10952|Mackunda Formation|68713|5|Briefly described|p22|Cretaceous|Cretaceous|||Of the Neales River Group.||||
10952|Mackunda Formation|68715|6|Mentioned|p30 Fig.7|Cenomanian|Albian|Eromanga Basin.||||||
10952|Mackunda Formation|68731|6|Mentioned|pp209-211|||||||||
10952|Mackunda Formation|68734|5|Briefly described|p218 Fig.2, p221 Fig.3|Cenomanian|Albian|Eromanga Basin (SW and NE). Marine to coastal paralic. Mis-spelt as Mackundra Formation in Fig.2.||Of the Rolling Downs Group.||||16-JAN-17
10952|Mackunda Formation|68821|5|Briefly described|p292 Fig.1, p296|Cretaceous|Cretaceous|Lower Cretaceous age. Parallic to marine sediments.||Of the Rolling Downs Group.||||
10952|Mackunda Formation|69019|4|Described|p83 Fig.20, p85, p99-101.|Cenomanian|Albian|Of Vine and Day (1965). Eromanga Basin; final Cretaceous marine deposition. Thickness from 0-192 m. Has developed a porcellanite horizon.||Unit in Neales River Group.||Overlies Oodnadatta Formation conformably; overlies Allaru Mudstone. Is overlain conformably by Winton Formation.|Pale grey-green, interbedded, glauconitic cross-bedded sand, silt; shale and calcareous shale, often as intraclasts in upper sand beds. Contains ovoidal limestone concretions to tabular limestone bodies.|
10952|Mackunda Formation|69023|5|Briefly described|p79, p86-87, p89 Fig.20, p93|Cenomanian|Albian|See also p105-106, p119, p122-123, p151, p191-192. Defined by Vine and Day (1965) in Queensland as the youngest marine to marginal marine unit within the Eromanga Basin. Thickness varies from <49 to ~82m. Marginal marine and paralic to deltaic. Diverse fauna listed. Weathering has formed porcellanite. Stratigraphic wells intersection data.||||Conformably overlies Oodnadatta Formation and Allaru Mudstone. Is overlain conformably by Winton Formation.|Pale grey-green, interbedded, glauconitic cross-bedded sand, silt, shale and calcareous shale. Local ferricrete capping.|
10952|Mackunda Formation|69457|4|Described|p41:2-3, 6-7, 10-12|Early Cretaceous|Early Cretaceous|Vine and Day (1965). Central and southern Eromanga Basin. Formerly part of the superseded Blanchewater Formation, used for the combined undifferentiated Mackunda-Winton Formations interval. Thickness is variable, from 74m to >150m. Marine; distinguished by its lack of coal. Contains a diverse fossil assemblage, from a dinosaur to microfossils.||Manuka Subgroup.||Conformably overlies Allaru Mudstone and Oodnadatta Formation. Is overlain conformably by Winton Formation.|Thinly interbedded labile very fine- to fine-grained lithic sandstone, laminated siltstone and mudstone with numerous plant remains, and lesser mud-clast intraformational conglomerate.|12-JUL-16
10952|Mackunda Formation|69562|6|Mentioned|p681-682|Mesozoic|Mesozoic|||Said to be a unit in Marree Subgroup.||||06-APR-22
10952|Mackunda Formation|69582|6|Mentioned|p65|Early Cretaceous|Early Cretaceous|Eromanga Basin.||||Overlies the Allaru Mudstone. Overrlain by the Winton Formation.||
10952|Mackunda Formation|69594|5|Briefly described|p519, p526, p530-531, p574|Cenomanian|Albian|Vine (1964); Vine and Day (1965). Eromanga Basin. Mostly 75-100+ metres thick. Boundaries in drill holes are distinguished by various geophysical properties (described). Shallow-marine and paralic deposits with abundant volcanilithic sediments from the E. Contains a distinct marine fauna (listed) including the "iconic" Muttaburrasaurus.||||Conformably overlies Allaru Mudstone. Is overlain conformably by Winton Formation.|Labile volcanic lithic-feldspathic interbedded sandstone, siltstone, mudstone and minor impure coquinitic and cone-in-cone limestone and intraformational conglomerate.|
10952|Mackunda Formation|69599|6|Mentioned|p599|Cretaceous|Cretaceous|||||Is overlain unconformably by Moses Sandstone.||
10952|Mackunda Formation|69673|5|Briefly described|p155 fig 127|Cretaceous|Cretaceous|||Manuka Subgroup||Overlies Oodnadatta Formation, Allaru Mudstone, overlain by Winton Formation|Carbonaceous, pyritic shale with lesser interbedded sandstone.|
10952|Mackunda Formation|69797|5|Briefly described|p17 Fig.2|Early Cretaceous|Early Cretaceous|Geol. Prov: Eromanga Basin.||||||
10952|Mackunda Formation|69946|4|Described|p23, p26-28, p57, p94, p123|Late Cretaceous|Early Cretaceous|Vine and Day (1965). Type section is at the headwaters of Mackunda Creek on Gnalta Station. 60 - 120m thick. Wireline log correlations.||||Conformably overlies Allaru Mudstone and Oodnadatta Formation. Is overlain conformably by Winton Formation.|Interbedded, partly calcareous very fine-grained sandstone, siltstone and shale. Locally, transgressive mudstone units are interbedded with shoreface sandstones.|
10952|Mackunda Formation|69947|6|Mentioned|p13 Fig.7.2|Late Cretaceous|Early Cretaceous|Eromanga Basin.||||||
10952|Mackunda Formation|69948|6|Mentioned|Fig.4.18|||Eromanga Basin.||||Overlies Allaru Mudstone. Is overlain by Winton Formation.||
10952|Mackunda Formation|70383|5|Briefly described|p45|Albian|Albian|Eromanga Basin. Marginal marine deposits.||||||
10952|Mackunda Formation|70821|5|Briefly described|p21, p33, p79-80|Late Cretaceous|Late Cretaceous|Eromanga Basin. Absent in the southern Thomson region. 30.5m thick in Mirintu 1 petroleum well. Hydrochemistry mentioned.||Rolling Downs Group.||Conformably overlies Allaru Mudstone. Is overlain by Winton Formation.||
10952|Mackunda Formation|70823|5|Briefly described|p25-p27, p41, p43-p44,p78|Early Cretaceous|Early Cretaceous|Eromanga Basin. Age is minimum depositional age. Up to 200m thick.|c. 101 Ma|||Overlies the Allaru Formation and the Oodnadatta Formation. Overlain by the Winton Formation.||
10952|Mackunda Formation|70824|5|Briefly described|p9|Cretaceous|Cretaceous|Eromanga Basin.||||Overlies the Allaru Mudstone. Overlain by the Winton Formation.||
10952|Mackunda Formation|70836|6|Mentioned|p474|Albian|Albian|Eromanga Basin.||||||
10952|Mackunda Formation|70860|6|Mentioned|p281|||Great Artesian Basin.||||||
10952|Mackunda Formation|71321|6|Mentioned|p15|||Of Eromanga Basin.||||Overlain by Winton Formation. Underlain by Mount Alexander Sandstone Member or Allaru Mudstone.||
10952|Mackunda Formation|71342|3|Fully described|Ch 1 p6, Ch 1 p19, Ch4 p25,|Cenomanian|Albian|Eromanga Basin. Defined by Vine and Day (1965) who nominated the type section at the headwaters of Mackunda Creek on Gnalta Station. Hosts a major confined aquifer. Up to 120m thick. Dated on the basis of palynology and rare macrofossils.Sedimentology and palaeoenvironment are discussed. Spore-pollen zone is given in Ch5 p57.  See also Ch5 p23, Ch5 p26-p28, Ch5 p33, Ch5 p57, Ch5 p125, Ch6 p8, Ch6 p10, Ch7 p13.||||Conformably overlies the Allaru Mudstone and the Oodnadatta Formation. Conformably overlain by the Winton Formation.|Interbedded, partly calcareous, very fine-grained sandstone, siltstone and shale.|
10952|Mackunda Formation|71855|5|Briefly described|p27|||||||Overlies the Toolebuc Formation.||
10952|Mackunda Formation|71863|5|Briefly described|p5|Cenomanian|Albian|Eromanga Basin.||||Overlies the Allaru Mudstone. Overlain by the Winton Formation.||
10952|Mackunda Formation|72298|5|Briefly described|p801|Cretaceous|Cretaceous|Eromanga Basin (SA,QLD,NSW). Note that it also appears as a unit in the Neales River Group. Upper part: confined aquifers, generally producing non-flowing artesian water bores.||Rolling Downs Group.||Overlies Oodnadatta FZ. Is overlain by Winton FZ.||
10952|Mackunda Formation|72456|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Marree 1:250k map sheet.|||||Sandstone, calcareous; siltstone and shale.|
10952|Mackunda Formation|73167|6|Mentioned|p664 Fig. 2|Cretaceous|Cretaceous|Eromanga Basin.||||||
10952|Mackunda Formation|73249|6|Mentioned|p319|Cretaceous|Cretaceous|Eromanga Basin.||||Overlies the Allaru Mudstone, underlies the Winton Formation.||
10952|Mackunda Formation|73251|6|Mentioned|p36, p62|Early Cretaceous|Early Cretaceous|Eromanga Basin, Frome Embayment. Marginal thermal maturity. Marginal marine.||||Underlain by Allura Mudstone. Underlain by and equivalent to Oodnadatta Formation.||
10952|Mackunda Formation|73343|6|Mentioned|p337|Cretaceous|Cretaceous|Eromanga Basin.||||Underlain by Allaru Mudstone. Equivalent to Winton Formation.||
10952|Mackunda Formation|73479|5|Briefly described|p156 Fig.2, p159-160, p166, p175|Cretaceous|Cretaceous|Eromanga Basin. Fluvial-lacustrine depositional environment. Significantly eroded following exhumation (late Cretaceous).|ca 97 Ma|||Overlies Allaru Mudstone, unconformably underlies Eyre Formation||
10980|Madigan Inlet Member|23539|5|Briefly described|p 467|||||||||
10980|Madigan Inlet Member|24465|4|Described|p348|Early Cambrian|Early Cambrian|Of Carrickalinga Head Formation (Keynes Subgroup). Maximum thickness at type section: 550m. Conformbly overlain by Blowhole Creek Member.||||||19-JAN-05
10980|Madigan Inlet Member|30377|4|Described|p204|||||||||
10980|Madigan Inlet Member|30378|6|Mentioned|p432|||||||||
10980|Madigan Inlet Member|30379|6|Mentioned|p90|||Unit of Carrickalinga Head Formation||||||
10980|Madigan Inlet Member|30381|6|Mentioned|Table 1|||||||||
10980|Madigan Inlet Member|40454|6|Mentioned|Table 1|||||||||
10980|Madigan Inlet Member|41947|5|Briefly described|p16|||||||||
10980|Madigan Inlet Member|42270|4|Described|p353|||See also Fig.4||||||
10980|Madigan Inlet Member|43759|4|Described|p446|||||||||
10980|Madigan Inlet Member|44133|5|Briefly described|p7 Fig. 7.4, 14, 15|Early Cambrian|Early Cambrian|Of the Carrickalinga Head Formation. Maximum Thickness: 1000m.||||||
10980|Madigan Inlet Member|60712|6|Mentioned|p30 Fig. 3|Early Cambrian|Early Cambrian|Of the Carrickalinga Head Formation (Daily and Milnes 1972, 1973). Name abandoned??||||||31-MAY-05
10980|Madigan Inlet Member|61307|5|Briefly described|p6 Fig. 3, p23|Cambrian|Cambrian|Of Carrickalinga Head Formation (Kanmantoo Group). Geological Province: Adelaide Fold Belt.||||||15-JAN-08
10980|Madigan Inlet Member|63848|4|Described|p531, p532 Fig.2, p534 Fig.4.|Early Cambrian|Early Cambrian|Contains poorly preserved brachiopods at Carrickalinga Head. Also contains, at Red Creek near Truro, several trace fossils including Helminthoidichnites and Psammichnites gigas.||Unit in Carrickalinga Head Formation.||Is overlain by Blowhole Creek Member.|Rippled, well-bedded, buff to grey, slightly calcareous sandstone; some siltstone and thin mudstone horizons.|
10980|Madigan Inlet Member|65892|5|Briefly described|p19-20.|Middle Cambrian|Middle Cambrian|Fleurieu Peninsula. Contains flame structures and water escape structures. Suggested deposition by sustained high-density turbidity currents coming from an active orogenic terrain in then-contiguous Antarctica.||Basal unit in Carrickalinga Head Formation.|||Series of units in which fine-grained, grey-green, poorly sorted sandstone grades upwards into olive-green mudstone.|
10987|Madura Formation|22663|5|Briefly described|S97-1 and 2 p3||Early Cretaceous|||||||01-MAR-10
10987|Madura Formation|22814|5|Briefly described|fig2|Cretaceous|Cretaceous|||||||
10987|Madura Formation|23989|5|Briefly described|p51|Cretaceous|Cretaceous|Geological Province: Officer Basin||||||03-MAR-10
10987|Madura Formation|24057|5|Briefly described|p97|Cretaceous|Cretaceous|Geological Basin: Eucla Basin.||||||
10987|Madura Formation|30012|4|Described|Table 1|||||||||
10987|Madura Formation|30268|6|Mentioned|p44|||||||||
10987|Madura Formation|30563|4|Described|p11|||Stratigraphic table on p7.||||||07-OCT-20
10987|Madura Formation|30564|5|Briefly described|p11|||||||||
10987|Madura Formation|30945|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
10987|Madura Formation|30975|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
10987|Madura Formation|31153|6|Mentioned|p111|||Refers bivalves of Eucla Basin.||||||
10987|Madura Formation|31562|6|Mentioned|p11|||Refers Lowry (1970)||||||
10987|Madura Formation|31902|4|Described|Table 1|||Fig.1||||||
10987|Madura Formation|31903|6|Mentioned|Map legend|Cretaceous|Cretaceous|Section only||||||
10987|Madura Formation|31904|4|Described|p7|||Table 1. Refers Fairbridge (1953), McWhae et al. (1958)||||||
10987|Madura Formation|31906|4|Described|p7|||Cretaceous. Table 1||||||
10987|Madura Formation|31907|4|Described|Table 1|||U. & L. Cret.||||||
10987|Madura Formation|31908|4|Described|Table 1|||U. & L. Cret.||||||
10987|Madura Formation|31909|3|Fully described|p7|||Formerly "Madura Shale". Type section||||||
10987|Madura Formation|31915|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
10987|Madura Formation|32552|2|Defined|p10|Cretaceous|Cretaceous|See also P37, 47, 49, 50-56 etc.||||||
10987|Madura Formation|32648|6|Mentioned|p32|||Cretaceous.||||||
10987|Madura Formation|32747|6|Mentioned|p365|||Comparison of sediments||||||
10987|Madura Formation|33586|4|Described|Table 1|||See also P13.||||||
10987|Madura Formation|33589|5|Briefly described|p10|||Cret.||||||
10987|Madura Formation|33592|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
10987|Madura Formation|33595|4|Described|Table 1|||||||||
10987|Madura Formation|34192|6|Mentioned|Map legend|Cenomanian|Albian|Cenomanian - Aptian||||||
10987|Madura Formation|34194|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
10987|Madura Formation|34742|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
10987|Madura Formation|34759|6|Mentioned|Fig.7|||Stratigraphy||||||
10987|Madura Formation|35496|4|Described|Table 1|||Also on p20.||||||07-OCT-20
10987|Madura Formation|36257|6|Mentioned|Table 2.1|||||||||
10987|Madura Formation|36701|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
10987|Madura Formation|36890|3|Fully described|p412|||Formerly Madura Shale||||||
10987|Madura Formation|36902|6|Mentioned|p24|||||||||
10987|Madura Formation|36915|6|Mentioned|Fig.7|||||||||
10987|Madura Formation|38221|6|Mentioned|Fig.4|||Great Australian Bight Basin||||||
10987|Madura Formation|38482|6|Mentioned|p24|||See also Table 11.||||||
10987|Madura Formation|39211|5|Briefly described|p69|||See Fig. 44||||||
10987|Madura Formation|39923|6|Mentioned|p354|||||||||
10987|Madura Formation|40992|6|Mentioned|Fig.23|||||||||
10987|Madura Formation|41751|3|Fully described|p1|||||||||
10987|Madura Formation|42108|4|Described|p319|||||||||
10987|Madura Formation|42315|6|Mentioned|p2|Aptian|Neocomian|||||||
10987|Madura Formation|42545|3|Fully described|p14|Aptian|Hauterivian|||||||
10987|Madura Formation|42959|5|Briefly described|p58 Fig.3|||||||||
10987|Madura Formation|43026|5|Briefly described|Table 1,p586|||||||||
10987|Madura Formation|43252|5|Briefly described|p163|||||||||
10987|Madura Formation|43498|6|Mentioned|8|Santonian|Neocomian|||||||
10987|Madura Formation|43814|6|Mentioned|Fig.3,p115|||||||||
10987|Madura Formation|44133|4|Described|p134|Aptian|Barremian|Previously known as 'Madura Shale'. Conformably overlies: Loongana Formation. Underlies disconformably the Hampton Sandstone. Overlain by Toondi Formation. Thickness: 474m.||||||
10987|Madura Formation|44145|4|Described|p549 fig 4-190, p553-4, p551, 559, 552|Aptian|Barremian|Eucla Basin. Base is time transgressive. Barremian or older onshore; latest Barremian offshore. Age from sparse flora & fauna. Type section in Transcontinental Railway 1 bore, Madura.||||Conformably overlies Loongana Sandstone. Grades northwards into Samuel Formation and Bejah Claystone.|Carbonaceous sandstone, siltstone, claystone and shale: commonly pyritic.|
10987|Madura Formation|44412|14|Not recorded|map legend||Cretaceous|Cret.||||||
10987|Madura Formation|45149|2|Defined|p60|Early Cretaceous|Early Cretaceous|See also Table 1 and p15.||||||07-OCT-20
10987|Madura Formation|45168|6|Mentioned|p6|||See also Table 1||||||
10987|Madura Formation|49060|5|Briefly described|Fig.15|||See also Fig. 5||||||
10987|Madura Formation|61197|5|Briefly described|p473, p475|Middle Cretaceous|Early Cretaceous|Eucla Basin. Continental to low-energy marine deposits. 0-120m thick.|||||Silt, clay/shale, carbonaceous sand; pyritic.|
10987|Madura Formation|61630|6|Mentioned|p555 Fig. 3|Early Cretaceous|Early Cretaceous|Geological Province: Eyre Sub-basin.||||||07-APR-09
10987|Madura Formation|62640|6|Mentioned|p73 Fig.7. |||||||Is overlain by Wilson Bluff Limestone.||
10987|Madura Formation|64580|4|Described|map legend||Early Cretaceous|Cross-bedded feldspathic sandstone, locally conglomeratic, carbonaceous sandstone; glauconitic sandstone, siltstone, claystone and shale; commonly pyritic.||||||09-DEC-08
10987|Madura Formation|65102|4|Described|p.366,369,375, Figs.4-41,4-53, Table4-15|Early Cretaceous|Early Cretaceous|Officer Basin. 6-951m; quartzose sandstone, glauconitic greensand & claystone; marine, mostly low energy; conformable on Loongana Sandstone; type section at Naries Point, 28deg 50min S, 124deg 52min E; contains sponges, trace fossils; Neocomian.||||||16-JUL-13
10987|Madura Formation|68715|6|Mentioned|p30 Fig.5|Barremian|Barremian|Bight Basin.||||||
10987|Madura Formation|69297|5|Briefly described|p14 fig 2.4, p25 fig 2.9, p60|Albian|Barremian|Eyre Sub-basin.||||Overlies the Loongana Formation. Overlain by the Ceduna Formation.|Shale.|
10987|Madura Formation|69598|5|Briefly described|p9, p11|Cretaceous|Cretaceous|Central Eucla Basin. Up to 274m thick. Contains potential seal lithologies.|||||Fluvial to marine claystones, carbonaceous mudstones, siltstones and sandstone.|
10987|Madura Formation|69632|5|Briefly described|p21 Tb.6, p26, p30, p32|Cretaceous|Cretaceous|Gunbarrel, Eucla Basins. Average shear-wave velocities tabulated. Palynomorphs indicate marine sedimentation for all but the base.||Bight Basin Group.||Overlies Loongana Formation.|Glauconitic, carbonaceous, pyritic sandstone, siltstone, grey claystone/shale, mudstone.|
10987|Madura Formation|69648|4|Described|p20-21, p38, map legend|Early Cretaceous|Early Cretaceous|Of Bight Basin margin. Occurs in drillholes. Maximum local thickness of 43 m. Explored for oil shale (with MVT-style lead and zinc as secondary targets) on BARTON and OOLDEA.||||Disconformably overlies Loongana Formation.|6 m of inter-tidal grey sandy silts (carbonaceous top 0.5 m) with some shale interclasts, greenish grey shale bands lower in section gradually becoming sandier and ferruginous towards base; grey to black, in part carbonaceous, mudstone and shale.|
10987|Madura Formation|70397|5|Briefly described|p3|Cretaceous|Cretaceous|Bight Basin.||||Unconformably overlain by Hampton Sandstone. Underlain by Loongana Sandstone.||29-JUL-19
10987|Madura Formation|70771|5|Briefly described|p2, p27|Cretaceous|Cretaceous|Eucla Basin.||||Conformably overlies the Loongana Formation. Unconformably overlain by the Hampton Sandstone.|Siliciclastic sedimentary rocks.|
10987|Madura Formation|70772|4|Described|p2, p4-p9, p12-17|Albian|Valanginian|Madura Shelf. The most laterally extensive and thickest unit of the onshore Bight Basin. Achieves a maximum thickness of at least 355m in Madura 1, thickness is measured at 256m in SDDH001; two wells, Eucla 1 and BN1 preserve anomalously thing sections. In NDDH002 and Eucla 1 it disconformably overlies crystalline basement. Thins in the west and east of the basin but remains thick in centre of the basin. Bioclasts are common in some places. Age is derived from palnological data from parts of the base and top of the formation. Deposited primarily in  a lacustrinel non-marine environment with some evidence of later marine influence. Charcoal, fossil brachiopods, cephalopds, shell fragments and dinocysts are present. See also  p22-26, p28, p31, p33-34, p36, p38, p40-41.||||Conformably overlies the Loongana Formation, disconformably overlies the Shanes Dam Conglomerate. Unconformably overlain by the Hampton Sandstone and the Eucla Group.|Fine sandy micaceous base with occasional charcoal rich horizons that grade into glauconitic medium to coarse sand. Overlying this is homogenous light grey siltstone and minor beds of fine sands.|
10987|Madura Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||siltstone, claystone, greensand|
10987|Madura Formation|71361|5|Briefly described|p5|Cretaceous|Cretaceous|Eucla Basin. Deposited in a marine environment when much of the Australian landmass was beneath the Eromanga Sea.||||Overlies the Loongana Sandstone. Unconformably overlain by the Hampton Sandstone.|Marine sandstones.|
10987|Madura Formation|71618|4|Described|p124-125,127-135,137|Albian|Early Cretaceous|Geological province: Bight Basin and Madura Shelf. Deposited during continued thermal subsidence and the most extensive unit in the Bight Basin. Depositional environment: non-marine, freshwater-brackish to intermittent marine. Thickness: at least 355m in Madura-1. Thickest in central basinal areas and generally thins toward basin margins. See p128 for isopachs. Samples from basal portions of the Madura Formation in both the HDDH001 (397.6-397.7 m) and FOR011 (256.8-257 m) yielded extremely similar assemblages to the Loongana Formation (Early Cretaceous) despite a separation of ~275 km. Uppermost sections in FOR011 (104.25-104.4 m) contained an extremely distinctive and rich dinocyst-dominated Albian palynomorph assemblage (Barham et al., 2016). U-Pb ICPMS zircon analysis yield major concordant age peaks at c. 1150 and 1650 Ma, similar to the Loongana Formation and Decoration Sandstone. Upper Madura Formation also yields a single concordant grain at c. 106 Ma, volcanic in origin and likely from an eruptive cloud from violent explosive eruptions around the Whitsundays.||||Disconformably overlain by Hampton Sandstone. Conformably underlain by Loongana Formation or disconformably underlain by Shanes Dam Conglomerate or crystalline basement.|Silts and fine sands, becoming increasingly glauconitic and bioturbated and fossiliferous at the top.|06-SEP-19
10987|Madura Formation|71891|5|Briefly described|p6-p7, p14, p29-p43, p45-p52, p54-p55|Late Cretaceous|Early Cretaceous|Bight basin, Coompana Province. 30-474m thick. Interpreted to have been deposited in a marine environment with limited circulation.||||Conformably overlies the Loongana Formation. Overlain by the Hampton Sandstone or Pidinga Formation unconformably.|Carbonaceous or glauconitic sandstone, siltstone, claystone and shale.|
10987|Madura Formation|72034|5|Briefly described|500k_interpgeop16_lut|Aptian|Barremian|Bight Basin.  Age from biostratigraphy.|||||Carbonaceous sandstone, siltstone, claystone and shale; commonly pyritic.|
10987|Madura Formation|72344|5|Briefly described|p4, p9, p13, p16, p49, p61|Early Cretaceous|Early Cretaceous|Bight Basin. Maximum thickness of 474m. Interpreted to have been deposited in a marine environment with limited circulation. Intersected in drillhole CDP008. Petrography, SHRIMP analyses and geochemistry are discussed for a sample. Maximum depositional age is derived from SHRIMP dating in this volume. See also p84, p96, p107-p108, p110, p114, p169.|1147 +/- 5 Ma (Max dep. Age)|||Conformably overlies the Loongana Formation.|Carbonaceous or glauconitic sandstone, siltstone and claystone and shale; commonly pyritic.|04-SEP-19
10987|Madura Formation|72465|5|Briefly described|p8, 17|Early Cretaceous|Early Cretaceous|Hill (1995). Bight Basin, Coompana Province. Up to 474m thick. Marine, low-energy lacustrine conditions.||||Conformably overlies Loongana Formation, or unconformably the Toolgana Supersuite.|Carbonaceous or glauconitic sandstone, siltstone, and claystone and shale; commonly pyritic.|
10987|Madura Formation|72466|5|Briefly described|p8, 17|Early Cretaceous|Early Cretaceous|Hill (1995). Bight Basin, Coompana Province. Up to 474m thick. Deposited in a marine, low-energy lacustrine environment.||||Conformably overlies Loongana Formation. Is overlain by Pidinga Formation.|Carbonaceous or glauconitic sandstone, siltstone, and claystone and shale; commonly pyritic.|
10987|Madura Formation|72467|5|Briefly described|p8, 17|Early Cretaceous|Early Cretaceous|Hill (1995). Bight Basin, Coompana Province. Up to 474m thick. Deposited in a marine, low-energy lacustrine environment.||||Conformably overlies Loongana Formation. Is overlain by Pidinga Formation.|Carbonaceous or glauconitic sandstone, siltstone, and claystone and shale; commonly pyritic.|
10987|Madura Formation|72468|5|Briefly described|p8, p17|Early Cretaceous|Early Cretaceous|Bight Basin. Maximum thickness of 474 m. Deposited in a marine environment with limited circulation suggested by low-energy lacustrine conditions.||||Conformably underlain by Loongana Formation.|Carbonaceous or glauconitic sandstone, siltstone, and claystone and shale; commonly pyritic.|
10987|Madura Formation|72469|5|Briefly described|p8, p17|Early Cretaceous|Early Cretaceous|Bight Basin. Maximum thickness of 474 m. Deposited in a marine environment with limited circulation suggested by low-energy lacustrine conditions.||||Conformably underlain by Loongana Formation.|Carbonaceous or glauconitic sandstone, siltstone, and claystone and shale; commonly pyritic.|
10987|Madura Formation|72470|5|Briefly described|p8, p18|Early Cretaceous|Early Cretaceous|Bight Basin. Maximum thickness of 474 m. Deposited in a marine environment with limited circulation suggested by low-energy lacustrine conditions.||||Conformably underlain by Loongana Formation.|Carbonaceous or glauconitic sandstone, siltstone, and claystone and shale; commonly pyritic.|
10987|Madura Formation|72471|5|Briefly described|p8, p17|Early Cretaceous|Early Cretaceous|Bight Basin. Maximum thickness of 474 m. Deposited in a marine environment with limited circulation suggested by low-energy lacustrine conditions.||||Conformably underlain by Loongana Formation.|Carbonaceous or glauconitic sandstone, siltstone, and claystone and shale; commonly pyritic.|
10987|Madura Formation|72472|4|Described|p8, p16-20|Early Cretaceous|Early Cretaceous|Bight Basin. Maximum thickness of 474 m. Deposited in a marine environment with limited circulation suggested by low-energy lacustrine conditions although observations from drillhole CDP008 indicate a non-marine setting. Interfingering transition with underlying Loongana Formation.||||Conformably underlain by Loongana Formation.|Carbonaceous or glauconitic sandstone, siltstone, and claystone and shale; commonly pyritic. Includes rip-up clasts of brown siltstone, irregular horizons of charcoal fragments, and red-brown medium to coarse grained sandstones and pebbly gravels.|
10987|Madura Formation|72947|6|Mentioned|p11|Cretaceous|Cretaceous|||||Overlies Koomalboogurra Suite.||
10987|Madura Formation|73084|5|Briefly described|p7, p16-19|Early Cretaceous|Early Cretaceous|Bight Basin. Typically between 150-200 m thick.||||Underlain by Loongana Formation and Shanes Dam Conglomerate. Unconformably[?] overlain by Hampton Sandstone.|Dark carbonaceous shale, siltstone and poorly consolidated minor sandstone.|
10987|Madura Formation|73232|6|Mentioned|p18|Early Cretaceous|Early Cretaceous|[May be] preserved in Eucla Basin palaeovalleys (Hou et al., 2008).||||||
10987|Madura Formation|73641|5|Briefly described|p4, 8-15, 17|Early Cretaceous|Early Cretaceous|Bight Basin. ~200m thick. Low-energy, limited circulation marine sedimentation. Mineralogical, element, TOC compositions tabulated.||||Overlies and interfingers with Loongana Formation.|Sandstones, carbonaceous sandstones, glauconitic sandstones, siltstones, and argillites, commonly pyritic.|
11147|Mampuwordu Sand|30056|6|Mentioned|Table 2|||||||||
11147|Mampuwordu Sand|41537|6|Mentioned|Fig.2|||||||||
11147|Mampuwordu Sand|42375|4|Described|p42|||Age Pliocene?||||||
11147|Mampuwordu Sand|42746|5|Briefly described|Fig.9 p14|||||||||21-SEP-18
11147|Mampuwordu Sand|43041|5|Briefly described|Fig.1,p590|||||||||
11147|Mampuwordu Sand|44133|5|Briefly described|p190 Fig. 10.30, 193|Late Miocene|Middle Miocene|Geoloigcal Province: Lake Eyre Basin. Of the Etadunna Formation.||||||
11147|Mampuwordu Sand|61155|5|Briefly described|p5, p17|Pliocene|Pliocene|Fluvial sandy deposits near Lake Eyre. Overlain by Tirari Formation. Age: 4.5-3.5Ma. Geological Province: Lake Eyre Basin.||||||
11147|Mampuwordu Sand|66131|5|Briefly described|p243, p244 Fig.4|Pliocene|Oligocene|Regarded as a channel facies of the Etadunna Formation. Age defined by that of the parent Formation.||Of the Etadunna Formation.||||
11147|Mampuwordu Sand|66573|6|Mentioned|p872|||See also references to superseded Mampuwordu Sands (p873, p874, p875 Tb.2, p876, p880 Fig.14).||||||
11147|Mampuwordu Sand|67462|5|Briefly described|Map legend.|Miocene|Miocene|Tirari Sub-basin, Lake Eyre Basin.||Unit in Etadunna Formation?||||04-DEC-13
11147|Mampuwordu Sand|68715|6|Mentioned|p30 Fig.5|Tortonian|Serravallian|Tirari and northern Callabonna sub basins, Lake Eyre Basin.||||||22-AUG-13
11169|Mangalo Schist|23285|5|Briefly described|Fig 3 p 333|||||||||
11169|Mangalo Schist|23719|4|Described|p14|Statherian|Statherian|See also page 14 Table 1. Also known as Cook Gap Schist. Age: 1688+/-76 Ma (Rb-Sr). Of Middleback Subgroup. O'lying unit Upper Middleback Jaspilite. U'lying unit Lower Middleback Jaspilite. Geol. Prov: Gawler Craton. Max. thickness: >1500 m.||||||
11169|Mangalo Schist|23791|6|Mentioned|p4|||||||||
11169|Mangalo Schist|39345|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
11169|Mangalo Schist|39349|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
11169|Mangalo Schist|39353|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
11169|Mangalo Schist|40448|6|Mentioned|Table 1|||||||||
11169|Mangalo Schist|41667|6|Mentioned|p53|||||||||
11169|Mangalo Schist|43052|5|Briefly described|p56|||see also Fig.4.4. Synonym for Cook Gap Schist.||||||27-FEB-15
11169|Mangalo Schist|62893|6|Mentioned|Map Legend, p10|Early Proterozoic|Early Proterozoic|Local name for the Cook Gap Schist in the Cleve Uplands region.||||||
11169|Mangalo Schist|66882|5|Briefly described|p103 Fig.3a,c; p105-107, p109-112|Statherian|Orosirian|Mount Bosanquet Region. Consists of outcrops formerly mapped as Cook Gap Schist W of Kalinjala Mylonite Zone. Geochemistry discussed.|1796+/-6 Ma and 1813+/-9 Ma|Cleve Group||Underlies Mount Shannon Iron Formation, disconformably overlies Darke Peak Group.||
11169|Mangalo Schist|67323|6|Mentioned|Eastern Australia Time-Space Plot|||Southern Gawler Craton.||||||
11169|Mangalo Schist|71348|6|Mentioned|p214-215|||Geological province: Gawler Craton. See p215 for summary of U-Pb geochronological data.||||||
11169|Mangalo Schist|71536|6|Mentioned|p79|||Correlated with the youngest rock (a mica-rich schist) in the Wilgerup sequence.||||||
11169|Mangalo Schist|73103|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Mentioned in the description of an amphibolite whose map symbol is L46, occurring ""only where not associated with Cook Gap/Mangalo Schist or Broadview Schist"".||||||
11169|Mangalo 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.||||||
11173|Mangaroongah Dacite|24474|3|Fully described|p38|||Of the Glyde Hill Volcanic Complex.  Ranges from basaltic andesite to porphyritic red-brown dacite.  Conformably overlies Childera Dacite; conformably underlies the Arburee Rhyolite.||||||
11173|Mangaroongah Dacite|30984|2|Defined|p15|Proterozoic|Proterozoic|||||||
11173|Mangaroongah Dacite|41974|6|Mentioned|p409|||||||||
11173|Mangaroongah Dacite|42546|5|Briefly described|Map legend|Mesoproterozoic||||||||
11173|Mangaroongah Dacite|42721|5|Briefly described|map legend|Carpentarian||||||||
11173|Mangaroongah Dacite|42722|5|Briefly described|map legend|Carpentarian|Carpentarian|Of the Glyde Hill Volcanic Complex.  Purplish-brown and purplish-grey porphyritic dacite, grading to rhyodacite; many pheocrysts of cream-coloured plagioclase, partly replaced by chlorite and epidote; upper part of unit more rhyodacitic and vesicular in p||||||07-APR-05
11173|Mangaroongah Dacite|42736|5|Briefly described|map legend|Mesoproterozoic||||||||
11173|Mangaroongah Dacite|43052|5|Briefly described|p111|||of Glyde Hill Volcanics Complex||||||
11173|Mangaroongah Dacite|43071|5|Briefly described|p13,Table 2|||of Gawler Range Volcanics||||||
11173|Mangaroongah Dacite|43094|4|Described|Table 4.|||of Glyde Hill Volcanic Complex||||||
11173|Mangaroongah Dacite|67909|5|Briefly described|p126-130|Mesoproterozoic|Mesoproterozoic|Lake Everard area. Volcanic textures and emplacement mechanism tabulated.||Glyde Hill Volcanic Complex.|||Includes intercalated layers of breccia.|
11173|Mangaroongah Dacite|69649|4|Described|p19-20|Mesoproterozoic|Mesoproterozoic|||Unit in Glyde Hill Volcanic Complex.||Conformably overlies Childera Dacite. Is overlain conformably by Arburee Rhyolite and Karkulta Rhyolite.|Basaltic andesite to porphyritic (15-20%) red-brown dacite.|24-FEB-15
11173|Mangaroongah Dacite|70659|5|Briefly described|p6-8|Mesoproterozoic|Mesoproterozoic|Misspelt as Manganroongah Dacite on p6.||Glyde Hill Volcanic Complex.|||Dacite separated by volcaniclastic intervals of tuffaceous mudstone, crystal and pumice rich sandstone and breccia.|
11173|Mangaroongah Dacite|70816|5|Briefly described|p5|||Lake Everard area, Gawler Ranges.||Unit of Glyde Hill Volcanic Complex.||Overlain by Karkulta Rhyolite. Underlain by Childera Dacite.||
11173|Mangaroongah Dacite|72090|6|Mentioned|p12|||Gawler Craton.||Glyde Hill Volcanic Complex||||
11184|Mann Metamorphics|32192|4|Described|p157|||1400-1600my||||||
11184|Mann Metamorphics|32548|6|Mentioned|p71|||Refers Thomson (1969)||||||
11184|Mann Metamorphics|32549|6|Mentioned|p56|||Refers Thomson (1969)||||||
11184|Mann Metamorphics|32550|6|Mentioned|p86|||||||||
11184|Mann Metamorphics|50607|6|Mentioned|p2.5|||||||||
11187|Mannum Formation|9124|5|Briefly described|Map Legend|Miocene|Oligocene|Sandy limestones.||||||
11187|Mannum Formation|22799|5|Briefly described|p23 Fig.7|Early Miocene|Early Miocene|||||||
11187|Mannum Formation|22887|5|Briefly described|Fig.6 p13|Early Miocene|Late Oligocene|||||||
11187|Mannum Formation|22893|5|Briefly described|fig4 p9|Miocene|Miocene|||||||
11187|Mannum Formation|22938|5|Briefly described|fig5|Miocene|Miocene|In the Eastern Mount Lofty Ranges.||||||30-JAN-08
11187|Mannum Formation|23179|6|Mentioned|Fig.2|Middle Miocene|Late Oligocene|Divided informally in SA into late Oligocene lower Mannnum Formation and early Miocene upper Mannum Formation. parent: Murray Supergroup.||||||
11187|Mannum Formation|23226|2|Defined|p891|Longfordian|Janjukian|Informally divided into upper and lower members; includes the Swan Reach Dolomite Member in upper section.  Of Murray Supergroup.||||||30-JAN-08
11187|Mannum Formation|23768|4|Described|p28 Fig.5, p33-34|Middle Miocene|Early Miocene|Underlies Morgan Limestone. Geological Province: Murray Basin.  See also p125, p157-158.||||||11-SEP-09
11187|Mannum Formation|23818|5|Briefly described|p173 Fig.84, p182|Early Miocene|Early Miocene|Geological Province: Murray Basin. Overlain by Finniss Clay.||||||30-JAN-08
11187|Mannum Formation|24551|6|Mentioned|p323|||||||||
11187|Mannum Formation|24558|4|Described|p655 Fig. 3|Early Miocene|Oligocene|Low energy carbonate ramp sediments with common echinoids, bryozoans and molluscs. Conformably underlies Finnis Formation.||||||29-JUL-08
11187|Mannum Formation|29591|6|Mentioned|Table 20|||||||||
11187|Mannum Formation|29697|5|Briefly described|Table 1|||||||||
11187|Mannum Formation|30514|6|Mentioned|p105|||See also P106. Lower Miocene age||||||
11187|Mannum Formation|30750|6|Mentioned|p3|||Tertiary age||||||
11187|Mannum Formation|30751|6|Mentioned|Map legend|Miocene|Miocene|||||||
11187|Mannum Formation|30753|4|Described|Table 2|||Lower Miocene age||||||
11187|Mannum Formation|30754|5|Briefly described|p13|||See also p14, 22. Stratigraphic table.||||||30-JAN-08
11187|Mannum Formation|30758|6|Mentioned|p66|||Stratigraphy. Important source of coarse aggregate||||||
11187|Mannum Formation|30807|6|Mentioned|p101|||Suggested map symbol||||||
11187|Mannum Formation|30828|6|Mentioned|p115|||||||||
11187|Mannum Formation|31516|6|Mentioned|Fig. 6|||Ammatocarcinus distribution||||||
11187|Mannum Formation|31625|6|Mentioned|Fig. 5.2|||Miocene||||||
11187|Mannum Formation|31746|6|Mentioned|p195|||||||||
11187|Mannum Formation|31848|4|Described|p14|||Age: Lower Miocene and Oligo-Miocene.||||||30-JAN-08
11187|Mannum Formation|31922|6|Mentioned|Fig.2|||||||||
11187|Mannum Formation|31923|6|Mentioned|p17|||||||||
11187|Mannum Formation|32401|6|Mentioned|p103|||||||||
11187|Mannum Formation|32404|6|Mentioned|p18|||||||||
11187|Mannum Formation|32426|6|Mentioned|p142|||Stratigraphic table. Renmark area||||||
11187|Mannum Formation|32432|6|Mentioned|Fig.2|||See also Table 1||||||
11187|Mannum Formation|32439|6|Mentioned|p99|||||||||
11187|Mannum Formation|32552|6|Mentioned|p84|||See also P184. Longfordian||||||
11187|Mannum Formation|32601|6|Mentioned|p672|||Type horizon for Paradoxechinus novus Laube||||||
11187|Mannum Formation|32653|6|Mentioned|p295|||||||||
11187|Mannum Formation|32862|5|Briefly described|Table 3|||||||||
11187|Mannum Formation|33224|6|Mentioned|Fig.35|||Photo||||||
11187|Mannum Formation|33826|6|Mentioned|p42|||Strat.table.||||||
11187|Mannum Formation|33834|5|Briefly described|p11|||||||||
11187|Mannum Formation|33982|6|Mentioned|p116|||||||||
11187|Mannum Formation|34029|5|Briefly described|Table 1|Early Miocene|Early Miocene|Aquifer. Lower Miocene.||||||30-JAN-08
11187|Mannum Formation|34114|4|Described|p50|||||||||
11187|Mannum Formation|34180|6|Mentioned|p212|||Tertiary||||||
11187|Mannum Formation|34248|6|Mentioned|p115|||||||||
11187|Mannum Formation|34296|5|Briefly described|p97|||||||||
11187|Mannum Formation|34308|4|Described|p180|||Correlation chart. Fig.84. Longfordian||||||
11187|Mannum Formation|34418|6|Mentioned|p506|||Equivalent||||||
11187|Mannum Formation|34421|6|Mentioned|p242|||See also PP243,244,259 etc||||||
11187|Mannum Formation|34460|6|Mentioned|Fig.3|||||||||
11187|Mannum Formation|34536|6|Mentioned|Map legend|Miocene|Miocene|||||||
11187|Mannum Formation|34758|6|Mentioned|Fig.2|||||||||
11187|Mannum Formation|34958|6|Mentioned|p88|||||||||
11187|Mannum Formation|35071|6|Mentioned|Table 1|||||||||
11187|Mannum Formation|35097|6|Mentioned|Fig.4|||||||||
11187|Mannum Formation|35200|6|Mentioned|Map legend|Miocene|Miocene|||||||
11187|Mannum Formation|35232|6|Mentioned|p11|||||||||
11187|Mannum Formation|35541|6|Mentioned|p12|||||||||
11187|Mannum Formation|36119|6|Mentioned|p58|||||||||
11187|Mannum Formation|37619|6|Mentioned|p2|||||||||
11187|Mannum Formation|38068|6|Mentioned|Fig.7|||||||||
11187|Mannum Formation|38070|6|Mentioned|Fig.12|||Murray Basin||||||
11187|Mannum Formation|38699|6|Mentioned|p8|||||||||
11187|Mannum Formation|39929|6|Mentioned|Fig.3|||||||||
11187|Mannum Formation|40003|5|Briefly described|p38|||||||||
11187|Mannum Formation|40820|6|Mentioned|Fig.4|||||||||
11187|Mannum Formation|41076|6|Mentioned|p56|||||||||
11187|Mannum Formation|41478|6|Mentioned|p86|||||||||
11187|Mannum Formation|41511|5|Briefly described|p18|||||||||
11187|Mannum Formation|41518|6|Mentioned|p146|||||||||
11187|Mannum Formation|41519|6|Mentioned|p168|||||||||
11187|Mannum Formation|41520|5|Briefly described|Fig.11|||||||||
11187|Mannum Formation|42125|5|Briefly described|p136|||||||||
11187|Mannum Formation|42127|5|Briefly described|p223|||||||||
11187|Mannum Formation|42130|6|Mentioned|Fig.3 P265|||||||||
11187|Mannum Formation|42134|6|Mentioned|Fig.3 P335|||||||||
11187|Mannum Formation|42137|6|Mentioned|p370|||||||||
11187|Mannum Formation|42138|6|Mentioned|Fig.2 P390|||||||||
11187|Mannum Formation|42371|6|Mentioned|p35, p41|||||||||
11187|Mannum Formation|42443|4|Described|p4|||||||||
11187|Mannum Formation|42473|6|Mentioned|p61|||||||||
11187|Mannum Formation|42499|5|Briefly described|Map legend|Miocene||||||||
11187|Mannum Formation|42717|5|Briefly described|map legend|Miocene||||||||
11187|Mannum Formation|42881|4|Described|Fig.3, P84|||||||||
11187|Mannum Formation|42966|2|Defined|Table 17, p128|Early Miocene|Late Oligocene|Of the Murray Group.||||||30-JAN-08
11187|Mannum Formation|43073|5|Briefly described|Table 3|||||||||
11187|Mannum Formation|43466|14|Not recorded|p3,Pl.1,fig.2|||Equivalent||||||
11187|Mannum Formation|43467|14|Not recorded|p3,19,25,31,32|||||||||
11187|Mannum Formation|43667|6|Mentioned|Fig.3,p12|Miocene|Oligocene|||||||
11187|Mannum Formation|43686|6|Mentioned|Fig.5,p233|||||||||
11187|Mannum Formation|43791|6|Mentioned|p372, Fig1|||||||||
11187|Mannum Formation|43804|6|Mentioned|Fig.2,p49|||||||||
11187|Mannum Formation|46802|6|Mentioned|Table 1|||||||||
11187|Mannum Formation|48971|6|Mentioned|p77|||||||||
11187|Mannum Formation|49038|5|Briefly described|p26|||||||||
11187|Mannum Formation|49040|6|Mentioned|p11|||||||||
11187|Mannum Formation|60785|5|Briefly described|p184 Fig.1, pp195-196.   |Burdigalian|Aquitanian|South Australia. Has yielded several fossil cetacean elements.|||||Yellow-orange calcarenite. Bryozoal calcarenite.|
11187|Mannum Formation|61155|5|Briefly described|p18|Early Miocene|Late Oligocene|Of the Murray Group. Overlies the Gambier Limestone; overlain by Finniss Clay. Age: ~24-20.5Ma. Thickness: 100m. Geological Province: Murray Basin.||||||25-MAY-06
11187|Mannum Formation|62899|6|Mentioned|p46, p48|Middle Miocene|Middle Miocene|In South Australia.||||||
11187|Mannum Formation|63460|4|Described|p839 Fig. 2b, p847|Early Miocene|Late Oligocene|Conformably overlies Ettrick Formation. Conformably overlain by Finniss Formation. Geological province: Murray Basin. Calcarenite, calcisiltite.||||||09-JUL-08
11187|Mannum Formation|63739|5|Briefly described|p46, p48|Middle Miocene|Middle Miocene|Contains ostracod assemblages in South Australia - eg. in Kingston-on-the-Murray.||||||01-JUL-08
11187|Mannum Formation|64237|5|Briefly described|p17, p18|Early Miocene|Late Oligocene|Part of the Ludbrook (1961) stratigraphic scheme for the Murray Group until 1995 when Rogers et al replaced it together with Morgan Limestone + Pata Limestone with the single unit, Mannum Limestone. Reinstated as Mannum Fm with reinstated Murray Gp.......||||||15-JUL-08
11187|Mannum Formation|65552|6|Mentioned|p5 Fig. 3|Miocene|Oligocene|Of Murray Group (western Murray Basin).||||||
11187|Mannum Formation|68715|5|Briefly described|p31 Fig.5|Burdigalian|Aquitanian|Murray Basin.||Of the Murray Group.||||
11187|Mannum Formation|70803|5|Briefly described|p24, p56, p60|Tertiary|Tertiary|Referred to as the Mannum Limestone on p24.|||||Fossiliferous marine limestone and calcareous sandstone.|
11187|Mannum Formation|72445|5|Briefly described|App.6 p1 Tb.1, p2 Fig.1, p6-7; App.7|Middle Miocene|Late Oligocene|Samples include bryozoans, molluscs and sponge spicules as well as benthic and planktic foraminifera in the Early Miocene M4 (17.54-16.39 Ma)and M5 (16.39-15.73 Ma) zones. App6 assigns the samples to upper Mannum Formation, but the well logs don't distinguish beyond Murray Group. Shown in App 7 Fig 4 (from Brown & Stephenson 1991).|Min age ~15.73 Ma from foraminifera.|Murray Supergroup/ Murray Group.||Overlies Renmark Group, Ettrick Formation. Underlies Finniss Formation. Shown as partially equivalent to Ettrick Formation.|Shown as limestone, App.7.|
11187|Mannum Formation|73118|6|Mentioned|p17|||||||||
11187|Mannum Formation|73188|6|Mentioned|p320|Miocene|Miocene|Murray Basin.||||||
11187|Mannum Formation|73228|4|Described|p50, p55-57|Middle Miocene|Early Miocene|Murray Basin. Deposited in shallow marine to littoral conditions.||Murray Group|||Cream to yellow-brown skeletal calcarenites, calcareous sandstone and sandy limestone, bryozoal limestone, marl, clay, and medium to coarse grained, sub-angular to well-rounded sand commonly cemented in a calcareous matrix.|
11187|Mannum Formation|73229|6|Mentioned|p66-67|Middle Miocene|Early Miocene|Murray Basin.||Murray Group||||
11189|Mannum Granite|23023|6|Mentioned|p1799||Arenig|Max Age: 481 (+/-) 9 Ma.||||||
11189|Mannum Granite|23317|6|Mentioned|378|||||||||
11189|Mannum Granite|23869|5|Briefly described|p15 Fig. 3|Ordovician|Ordovician|||||||
11189|Mannum Granite|24593|5|Briefly described|p629|||Age: 482+/-4.5 (Rb-Sr) and 442+/-3Ma (U/Pb).  Geological Province: Adelaide Fold Belt.||||||
11189|Mannum Granite|42275|5|Briefly described|p479|||Note: Mannum Formation and Mannum Limestone also used in SA.||||||
11189|Mannum Granite|44133|5|Briefly described|p51 Fig. 7.18, 55, 56 Table 7.3|Ordovician|Ordovician|A-Type. Medium to coarse grained biotite granite. Age: 481 +/- 9Ma. A-Type.||||||
11189|Mannum Granite|67536|5|Briefly described|Map Legend|Darriwilian|Stage 3|Kanmantoo Province; basement to Murray Basin.|ca. 497 +/- 10 Ma - 471 +/- 12 Ma||||Late/post-Delamerian felsic intrusive rocks.|
11189|Mannum Granite|68314|5|Briefly described|p754, p756, p759|Ordovician|Ordovician|Anorogenic: intrusion occurred soon after end of Delamerian deformation. Age inferred from Fig.5.|c.485 Ma.|||||
11189|Mannum Granite|70382|6|Mentioned|p34|Early Ordovician|Cambrian|Felsic intrusive magmatic phase during the late stages of, and immediately post-dating Cambrian Delamerian Orogeny (Foden et al., 2002, 2006; Preiss 1995).|~510-480 Ma||||A-type granite.|
11189|Mannum Granite|71322|5|Briefly described|p52 Fig.1|Ordovician|Cambrian|Late/post Delamerian.|497+/-10 Ma - 471+/-2 Ma.||||Felsic intrusive rocks.|
11189|Mannum Granite|73430|6|Mentioned|p493 Fig.2, p495|Early Ordovician|Early Ordovician|A-type granite. Also written as Mannum granite p495.|482.7+/-2 Ma LA-ICP-MS zircon U-Pb|Padthaway Ridge suite|||Granite.|
11215|Manuka Subgroup|13516|6|Mentioned|p167 fig 10, p169 fig 11|Late Cretaceous|Late Cretaceous|Eromanga Basin.||Of Rolling Downs Group||||
11215|Manuka Subgroup|29591|6|Mentioned|p69|||||||||
11215|Manuka Subgroup|39445|6|Mentioned|Table 11|||||||||
11215|Manuka Subgroup|63979|5|Briefly described|p53|||Of Rolling Downs Group. Includes Mackunda and Winton Formations.||||||07-FEB-11
11215|Manuka Subgroup|69457|5|Briefly described|p41:6, 11-13|Early Cretaceous|Early Cretaceous|Vine et al. (1967). Eromanga Basin.||Rolling Downs Group.|Mackunda and Winton Formations.|Overlies Wilgunya and Marree Subgroups.||12-JUL-16
11215|Manuka Subgroup|69673|6|Mentioned|p156||||||Includes Mackunda Formation, Winton Formation|Overlies Wilgunya Subgroup||
11262|Marcollat Granite|23869|5|Briefly described|p15 Fig. 3|Ordovician|Ordovician|||||||
11262|Marcollat Granite|42275|5|Briefly described|p476|||See also Fig.1, Table 3||||||
11262|Marcollat Granite|42549|5|Briefly described|p156|||||||||
11262|Marcollat Granite|44133|5|Briefly described|p51 Fig. 7.18, 55, 56 Table 7.3|Ordovician|Ordovician|A-Type.||||||
11262|Marcollat Granite|73093|5|Briefly described|map legend|Ordovician|Cambrian||||||Granite, green to olive-green, coarse-grained; hornblende-biotite. A-type, post-tectonic.|09-DEC-21
11262|Marcollat Granite|73430|6|Mentioned|p495|Early Ordovician|Early Ordovician|A-type granite.|478.2+/-0.8 Ma LA-ICP-MS zircon U-Pb|Padthaway Ridge suite|||Granite.|
11374|Marree Subgroup|13497|5|Briefly described|p115, p115 fig 6.33|Early Cretaceous|Early Cretaceous|Eromanga Basin.|||Includes the Wallumbilla Formation, Toolebuc Formation, Allaru Mudstone, Mackunda Formation, Bulldog Shale, Coorikiana Sandstone and the Oodnadatta Formation.|||
11374|Marree Subgroup|13516|5|Briefly described|p167 fig 10, p171 fig 12|Early Cretaceous|Early Cretaceous|In Eromanga Basin.|||Includes Bulldog Shale, Coorikiana Sandstone, Oodnadatta Formation|||
11374|Marree Subgroup|22883|5|Briefly described|Fig2 p30||Early Cretaceous|Overlying unit is Mackunda Formation, underlying unit is Cadna-owie Formation||||||05-OCT-06
11374|Marree Subgroup|23154|6|Mentioned|Map Legend|Late Cretaceous|Early Cretaceous|Geological Province - Eromanga Basin. Parent - Neales River Group.||||||
11374|Marree Subgroup|23155|5|Briefly described|p30|Early Cretaceous|Early Cretaceous|||||||
11374|Marree Subgroup|24175|5|Briefly described|p16, p17 Fig. 3|Albian|Aptian|Supersedes Marree Formation. See also p23. Geological Province: Eromanga Basin.||||||05-OCT-06
11374|Marree Subgroup|24210|5|Briefly described|p133 Fig. 2|Early Cretaceous|Early Cretaceous|Geological Province: Eromanga Basin.||||||
11374|Marree Subgroup|24321|5|Briefly described|Map legend|Albian|Barremian|Of the Neales River Group.||||||05-OCT-06
11374|Marree Subgroup|36494|6|Mentioned|p155|||||||||
11374|Marree Subgroup|36895|4|Described|p11|||||||||
11374|Marree Subgroup|38022|6|Mentioned|p9|||||||||
11374|Marree Subgroup|38604|6|Mentioned|Map legend|Aptian|Aptian|||||||
11374|Marree Subgroup|39352|6|Mentioned|Map legend|Albian|Aptian|Aptian to Albian||||||
11374|Marree Subgroup|39629|6|Mentioned|Fig.1|||||||||
11374|Marree Subgroup|40670|6|Mentioned|Fig.9|||||||||
11374|Marree Subgroup|40911|6|Mentioned|Map legend|Albian|Neocomian|||||||
11374|Marree Subgroup|40914|6|Mentioned|Map legend|Mesozoic|Mesozoic|||||||
11374|Marree Subgroup|40925|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
11374|Marree Subgroup|40926|6|Mentioned|Table 2|||||||||
11374|Marree Subgroup|41085|3|Fully described|p89|||||||||
11374|Marree Subgroup|41086|3|Fully described|p98|||||||||
11374|Marree Subgroup|41088|6|Mentioned|Fig.2|||||||||
11374|Marree Subgroup|41098|5|Briefly described|p175|||||||||
11374|Marree Subgroup|41125|6|Mentioned|p34|||||||||
11374|Marree Subgroup|41165|6|Mentioned|Fig.3|||||||||
11374|Marree Subgroup|41175|6|Mentioned|Fig.3|||||||||
11374|Marree Subgroup|41216|6|Mentioned|Fig.18|||||||||
11374|Marree Subgroup|42346|5|Briefly described|p77|Early Cretaceous||Informally divided into 3 subgroups 'Kopi', 'Mud','Bulldust'.||||||
11374|Marree Subgroup|42375|5|Briefly described|Fig. 26 P120||Cretaceous|||||||
11374|Marree Subgroup|42465|5|Briefly described|Map Legend|||||||||
11374|Marree Subgroup|42746|4|Described|p11|||See also Fig.2||||||
11374|Marree Subgroup|42905|5|Briefly described|Fig 5.3|||||||||
11374|Marree Subgroup|43085|5|Briefly described|Fig.5|||||||||
11374|Marree Subgroup|44133|4|Described|p117|Mesozoic|Mesozoic|Comprises Bulldog Shale, Coorikiana Sandstone and Oodnadatta Formation.  Geological Province: Eromanga Basin. Formerly named Marree Formation. Of the Neales River Group.||||||
11374|Marree Subgroup|44289|5|Briefly described|Map Legend|||||||||
11374|Marree Subgroup|44934|5|Briefly described|Map Legend||Cretaceous|||||||
11374|Marree Subgroup|44935|5|Briefly described|Map Legend||Aptian|||||||
11374|Marree Subgroup|60955|5|Briefly described|Map Legend|Cretaceous|Jurassic|Includes Bulldog Shale, Cadna-owie Formation and Algebuckina Sandstone. White, kaolinitic siltstones with erratic rounded boulders; gravels, conglomerates. Shales and carbonaceous clays, lignite.||||||13-APR-05
11374|Marree Subgroup|61615|6|Mentioned|p302 Fig. 2|Early Cretaceous|Early Cretaceous|Includes; Bulldog Shale, Allaru Mudstone, Wallumbilla and Toolebuc Formations and Coorikiana Sandstone. Geological Province: Eromanga Basin.||||||07-FEB-11
11374|Marree Subgroup|63102|5|Briefly described|p62,72|Cretaceous|Cretaceous|Geological province: Olary Domain, Curnamona Province. Restricted to the northern part of Curnamona Province.|||||Fine clastics and dark green-grey to grey, silty and sandy shale which in places is finely laminated and carbonaceous.|22-OCT-19
11374|Marree Subgroup|64197|6|Mentioned|p625 Fig.1c, p630 Fig.6|Early Cretaceous|Early Cretaceous|Eromanga Basin. Appears only as 'Maree' in Fig.1c.|||Includes Oodnadatta Formation, Allaru Mudstone, Toolebuc Formation, Bulldog Shale, Coorikiana Sandstone and Wallumbilla Formation.|Overlies Cadna-owie Formation; is overlain by Mackunda Formation.||
11374|Marree Subgroup|65376|5|Briefly described|p9 Fig.1.2. |Cretaceous|Cretaceous||||||Marine mudstone and sandstone.|
11374|Marree Subgroup|65689|6|Mentioned|p154|Cretaceous|Cretaceous|Eromanga Basin.|||Includes Bulldog Shale.|||
11374|Marree Subgroup|65925|5|Briefly described|Appendix 2.||||||||Dark grey, bioturbated, fossiliferous shale; fine- to very fine-grained, calcareous, clayey sandstone.|
11374|Marree Subgroup|66518|5|Briefly described|p19 Fig.4.|Cretaceous|Cretaceous|Eromanga Basin.|||Includes Bulldog Shale, Coorikiana Sandstone and Oodnadatta Formation.|Overlies Parabarana Sandstone and Cadna-owie Formation. Is overlain by Mackunda Formation.||
11374|Marree Subgroup|66623|6|Mentioned|p258.|||Laterally equivalent to Wallumbilla Formation in NSW.||Unit in Neales River Group.||||
11374|Marree Subgroup|68068|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Eromanga Basin. Commonly silcreted.||Unit in Neales River Group.|Includes Bulldog Shale, Coorikiana Sandstone and Oodnadatta Formation.|Conformably overlies Parabarana Sandstone. Is overlain conformably by Mackunda Formation.|Laminated marine shale, silt and clay; bioturbated, dark grey, with occasional shelly beds.|
11374|Marree Subgroup|68713|5|Briefly described|p22|Cretaceous|Cretaceous|||Of the Neales River Group.|Includes Bulldog Shale, Coorikiana Sandstone, and Oodnadatta Formation.|||
11374|Marree Subgroup|68715|6|Mentioned|p30 Fig.5|Albian|Aptian|Billa Kalina Basin.||||||
11374|Marree Subgroup|69019|5|Briefly described|p83 Fig.20, p85, p93-103.|Cretaceous|Cretaceous|Of Thomson (1980); formerly Marree Formation (Forbes et al., 1965 and Forbes, 1966).||Unit in Neales River Group.|Includes Bulldog Shale, Coorikiana Sandstone and Oodnadatta Formation.||Dark grey laminated shale, with or without silt and/or clay; locally bioturbated; contains shelly beds, limestone concretions and cone-in-cone limestone pods.|
11374|Marree Subgroup|69023|4|Described|p79, p86-87, p93, p99-104,p106, p110-111|||See also p116, p119, p143-144, p151, p159-160, p191-192. Eromanga Basin. Of Thomson (1980); formerly Marree Formation of Forbes et al. (1965); Forbes (1966). The term Marree Subgroup is used for the shaly sequence where Coorikiana Sandstone is absent. Weathering has formed porcellanite. Stratigraphic wells intersection data.|||Includes Bulldog Shale, Coorikiana Sandstone and Oodnadatta Formation.|Overlies Cadna-owie Formation. Is overlain by Winton and Mackunda Formations.|Local ferricrete capping.|
11374|Marree Subgroup|69457|5|Briefly described|p41:6-8|||Forbes (1966); Thomson (1980). SW Eromanga Basin. This Subgroup's nomenclature is less appropriate (than the Wilgunya Subgroup) in the NT, where the Coorikiana Sandstone has not been recognised.||Rolling Downs Group.|Bulldog Shale, Coorikiana Sandstone, Oodnadatta Formation.|Equivalent to Wilgunya Subgroup. Is overlain by Manuka Subgroup.||12-JUL-16
11374|Marree Subgroup|69562|5|Briefly described|p679, p680-682, p684|Mesozoic|Mesozoic|Eromanga Basin.|||Includes Mackunda and Oodnadatta Formations and Bulldog Shale.|Is overlain by Eyre Formation.|Highly conductive pyritic black muds.|
11374|Marree Subgroup|69654|6|Mentioned|p4|||Curnamona Province.||||||
11374|Marree Subgroup|69946|5|Briefly described|p23, p94|||Eromanga Basin. This name is applied to the shaly marine sequence (Bulldog Shale-Oodnadatta Formation) when the Coorikiana Sandstone is absent.|||Includes Bulldog Shale, Coorikiana Sandstone and Oodnadatta Formation.|Passes laterally into Oodnadatta Formation.||
11374|Marree Subgroup|69947|5|Briefly described|p9, p13 Fig.7.2|Early Cretaceous|Early Cretaceous|Eromanga Basin. On p9 the authors state: "the fluviolacustrine Winton Formation of the upper Marree Subgroup", which contradicts what appears in Fig.7.2.|||Bulldog Shale; Wallumbilla, Toolebuc, Oodnadatta Formations; Coorikiana Sandstone; Allaru Mudstone.|||
11374|Marree Subgroup|70336|5|Briefly described|Map legend|Cretaceous|Cretaceous||||Oodnadatta Formation, Coorikiana Sandstone, Bulldog Shale.||Dark grey, bioturbated, fossiliferous shale; fine- to very fine-grained, calcareous, clayey sandstone.|
11374|Marree Subgroup|70384|5|Briefly described|Map legend.|Albian|Cretaceous|Eromanga Basin.||Neales River Group.|Bulldog Shale, Coorikiana Sandstone.|Overlies Cadna-owie Formation.|Undifferentiated: dark grey shale, laminated +/- silt +/- clay, bioturbated, occasional shelly beds, limestone concretions and cone-in-cone limestone pods.|24-JAN-19
11374|Marree Subgroup|70657|5|Briefly described|p68, p77-78|Cretaceous|Cretaceous|Callabonna Sub-basin, northern Curnamona Province.|||||Fine clastics and dark green-grey to grey, silty and sandy shale which in places is finely laminated and carbonaceous.|
11374|Marree Subgroup|71342|5|Briefly described|Ch4 p8, Ch5 p23, Ch7 p9, Ch7 p13|Albian|Albian|Deposited in a marine depositional environment.|||Includes the Bulldog Shale, Coorikiana Sandstone and the Oodnadatta Formation.||Shales and mudstones.|
11374|Marree Subgroup|72456|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Marree 1:250k map sheet.|||||Shale, dark-grey, bioturbated, fossiliferous; sandstone, fine to very fine-grained, calcareous and clayey.|
11374|Marree Subgroup|73099|5|Briefly described|Map legend.|Early Cretaceous|Early Cretaceous|Eromanga basin.||Neales River Group.|Cadna-owie Formation, Bulldog Shale.|Overlies Cadna-owie Formation.||
11587|Meadows Sandy Loam|38290|5|Briefly described|p60|||||||||
11654|Mepunga Formation|22587|6|Mentioned|p79 Fig.7|Late Eocene|Middle Eocene|of the Nirranda Group||||||
11654|Mepunga Formation|22674|5|Briefly described|Fig.2 p719|Middle Eocene|Middle Eocene|||||||
11654|Mepunga Formation|22875|3|Fully described|p59|Early Oligocene|Eocene|Of the Nirranda Group.||||||07-MAR-07
11654|Mepunga Formation|22944|5|Briefly described|Fig3|Oligocene|Eocene|||||||
11654|Mepunga Formation|23230|5|Briefly described|Table4-1p40||Eocene|||||||
11654|Mepunga Formation|23238|5|Briefly described|p106||Tertiary|||||||
11654|Mepunga Formation|23322|5|Briefly described|957 Fig.2|Middle Eocene|Middle Eocene|Of the Nirranda Group.  Geological Province: Gambier Basin.||||||07-SEP-09
11654|Mepunga Formation|24200|5|Briefly described|p411|Oligocene|Eocene|Geological Province: Otway Basin.||||||
11654|Mepunga Formation|24314|5|Briefly described|p61 Fig.2|Middle Eocene|Middle Eocene|Geological Province: Otway Basin. Of the Nirranda Group.||||||
11654|Mepunga Formation|24397|5|Briefly described|p245|Late Eocene|Late Eocene|Geological Province: Otway Basin.||||||
11654|Mepunga Formation|24455|6|Mentioned|p327|||Overlain unconformably in some areas by Dilwyn Formation.||||||22-MAR-05
11654|Mepunga Formation|24551|5|Briefly described|p246, 296, p292 Fig. 10.3|Eocene|Eocene|Of the Nirrandra Group.  Max thickness: 160m.||||||
11654|Mepunga Formation|24562|5|Briefly described|p7,8 Fig.2|Eocene|Eocene|Conformably underlies Narrawaturk Marl.  Geological Province: Otway Basin.  Of the Nirranda Group.||||||07-MAR-07
11654|Mepunga Formation|29823|6|Mentioned|p14|||||||||
11654|Mepunga Formation|29825|5|Briefly described|p18|||||||||
11654|Mepunga Formation|29856|6|Mentioned|p36|||||||||
11654|Mepunga Formation|30576|5|Briefly described|Table 2|||||||||
11654|Mepunga Formation|30578|6|Mentioned|p9|||||||||
11654|Mepunga Formation|30580|6|Mentioned|Map legend|Eocene|Eocene|||||||
11654|Mepunga Formation|30675|5|Briefly described|p253|||||||||
11654|Mepunga Formation|30676|5|Briefly described|p12|||||||||
11654|Mepunga Formation|30932|6|Mentioned|Map legend|Eocene|Eocene|Part of Heytesbury Group.||||||20-SEP-07
11654|Mepunga Formation|31036|5|Briefly described|p194|||See also Table 9-1, p210. Unit of Nirranda Group.||||||07-MAR-07
11654|Mepunga Formation|31245|4|Described|p81|||See also p82. M.-U. Eocene.||||||07-MAR-07
11654|Mepunga Formation|31372|6|Mentioned|p12|||||||||
11654|Mepunga Formation|31424|4|Described|p14|||See also p7. Described from core.||||||07-MAR-07
11654|Mepunga Formation|31534|6|Mentioned|p363|||See also Table 19-1 ? aquifer in well. Water analysis.||||||
11654|Mepunga Formation|31625|6|Mentioned|Fig. 5.2|||Eocene||||||
11654|Mepunga Formation|32852|6|Mentioned|p10|||||||||
11654|Mepunga Formation|33155|5|Briefly described|p122|||||||||
11654|Mepunga Formation|33940|6|Mentioned|p414|||||||||
11654|Mepunga Formation|34063|6|Mentioned|p2|||Table. Upper Eocene.||||||20-SEP-07
11654|Mepunga Formation|34360|6|Mentioned|p11|||||||||
11654|Mepunga Formation|35066|4|Described|p209|||||||||
11654|Mepunga Formation|35285|6|Mentioned|p414|||||||||
11654|Mepunga Formation|35772|6|Mentioned|p9|||||||||
11654|Mepunga Formation|36913|6|Mentioned|p79|||||||||
11654|Mepunga Formation|37548|6|Mentioned|p131|||||||||
11654|Mepunga Formation|38625|6|Mentioned|Fig.2|||||||||
11654|Mepunga Formation|38932|4|Described|p98|||||||||
11654|Mepunga Formation|40003|5|Briefly described|p44|||See also Table 10||||||
11654|Mepunga Formation|40560|6|Mentioned|p6|||||||||
11654|Mepunga Formation|41185|6|Mentioned|Fig.4|||||||||
11654|Mepunga Formation|41269|5|Briefly described|p246|||||||||
11654|Mepunga Formation|41517|6|Mentioned|p134|||See also P139||||||
11654|Mepunga Formation|41642|6|Mentioned|Fig.8.6|||||||||
11654|Mepunga Formation|41701|6|Mentioned|Map legend|Oligocene||||||||
11654|Mepunga Formation|41704|6|Mentioned|Fig.3|||||||||
11654|Mepunga Formation|41714|6|Mentioned|Fig.2|||||||||
11654|Mepunga Formation|41726|6|Mentioned|Fig.5|||||||||
11654|Mepunga Formation|41769|4|Described|p25|||||||||
11654|Mepunga Formation|41868|5|Briefly described|p535|||||||||
11654|Mepunga Formation|42318|6|Mentioned|Fig.2 P10|||||||||
11654|Mepunga Formation|42453|6|Mentioned|p11|||Port Campbell Embayment||||||
11654|Mepunga Formation|42524|5|Briefly described|Fig.3 P27|||||||||
11654|Mepunga Formation|42601|6|Mentioned|Fig.2 p15|||||||||
11654|Mepunga Formation|42827|5|Briefly described|p283|||Of Nirranda Sub-group.||||||07-MAR-07
11654|Mepunga Formation|42863|5|Briefly described|Fig.14|||Variation on Victorian unit.||||||
11654|Mepunga Formation|43171|6|Mentioned|5-8|||Of Nirranda Group. Age: 40-45Ma||||||12-SEP-18
11654|Mepunga Formation|43195|5|Briefly described|Map Legend||Middle Eocene|See also commentary on back of map. Of Nirranda Group.||||||
11654|Mepunga Formation|43208|5|Briefly described|map legend|Early Oligocene|Middle Eocene|||||||
11654|Mepunga Formation|43219|5|Briefly described|Fig.3,p6.||Eocene|Of Nirranda Group.||||||07-MAR-07
11654|Mepunga Formation|43590|4|Described|p21|Early Oligocene|Middle Eocene|||||||
11654|Mepunga Formation|43660|6|Mentioned|Fig.6,p15|Oligocene|Eocene|||||||
11654|Mepunga Formation|43667|6|Mentioned|Fig.3,p12||Middle Eocene|||||||
11654|Mepunga Formation|43733|6|Mentioned|Fig.2.11,p65||Eocene|||||||
11654|Mepunga Formation|43744|6|Mentioned|Fig.3,p3|||||||||
11654|Mepunga Formation|43814|6|Mentioned|Fig.3,p115|||||||||
11654|Mepunga Formation|43937|5|Briefly described|Map Legend|Middle Eocene|Paleocene|||||||
11654|Mepunga Formation|44133|4|Described|p155|Late Eocene|Middle Eocene|Of the Nirranda Group. Geological Province: Gambier Basin. Thickness: 12m. Conformably underlies Narrawaturk Marl.||||||20-SEP-07
11654|Mepunga Formation|48911|6|Mentioned|Chart 1|||||||||
11654|Mepunga Formation|48977|6|Mentioned|Fig.5|||||||||
11654|Mepunga Formation|60563|6|Mentioned|p47|||||||||
11654|Mepunga Formation|61155|5|Briefly described|p3, p18|Early Oligocene|Middle Eocene|Of the Nirranda Group. Calcareous sands.Partly interfingers with Demons Bluff Formation. Max. thickness: 380m. Geological Province: Otway Basin.||||||07-MAR-07
11654|Mepunga Formation|61182|3|Fully described|p25-26, p33|Early Oligocene|Middle Eocene|Of Nirranda Gp. Variously interpreted based on its sand and mudstone units. The Sturgess Point Mbr has two informally named units, the upper and lower Mepunga sands, above and below it. Disconformable over Dilwyn Fm; conformable below the Narrawaturk Marl||||||04-FEB-08
11654|Mepunga Formation|61547|6|Mentioned|p461 Fig.2. |Eocene|Eocene|||Unit in Nirranda Group.||Is overlain by Narrawaturk Marl.||
11654|Mepunga Formation|61623|6|Mentioned|p449 Fig. 4|Oligocene|Eocene|Of Nirranda Group. Geological Province: Otway Basin.||||||07-APR-09
11654|Mepunga Formation|61624|6|Mentioned|p466 Fig. 2|Oligocene|Eocene|Of Nirranda Group. Geological Province: Otway Basin.||||||07-APR-09
11654|Mepunga Formation|61626|5|Briefly described|p486, p486 Fig. 2, p488 Fig. 4|Eocene|Eocene|Of Nirranda Group. Geological Province: Otway Basin.||||||07-APR-09
11654|Mepunga Formation|61628|5|Briefly described|p509 Fig. 3|Early Oligocene|Middle Eocene|Of Nirranda Group. Geological Province: Otway Basin.||||||07-APR-09
11654|Mepunga Formation|63124|3|Fully described|p87 Fig. 5.29, p90-91|Middle Eocene|Middle Eocene|Of Nirranda Group. Unconformably overlies Dilwyn Formation; conformably overlain by Narrawaturk Marl and Greenways Member of Gambier Limestone. Age: 46-39.5Ma. Thickness: ~12m. Geol.prov: Gambier Basin. Synonymous with Kongorong Sand (Ludbrook 1971).||||||31-JAN-08
11654|Mepunga Formation|63269|5|Briefly described|p605|Oligocene|Eocene|Otway Basin.||Nirranda Group.||||
11654|Mepunga Formation|63431|5|Briefly described|p677 Fig. 2|Eocene|Eocene|Of the Nirranda Group. Geological Province: Penola Trough/Otway Basin.||||||07-FEB-11
11654|Mepunga Formation|65891|6|Mentioned|p221 Fig.5. |Paleogene|Paleogene|Central Otway Basin. Includes Sturgess Point Member. Age shown as Bartonian to Priabonian.||||||
11654|Mepunga Formation|66002|5|Briefly described|p10 Tb.7, p16, p26 Fig.7, p58|Paleogene|Paleogene|Of Nirranda Group. Overlies Dilwyn Formation. Underlies Narrawaturk Marl. Similar to Wiridjil Gravel, and therefore some outcrops reassigned to Wiridjil herein.||||||
11654|Mepunga Formation|66245|6|Mentioned|p6 Fig.5. |Priabonian|Lutetian|||Unit in Nirranda Group.||||
11654|Mepunga Formation|67061|6|Mentioned|p546 Fig.3.|Eocene|Eocene|||Unit in Nirranda Group.||||
11654|Mepunga Formation|67366|5|Briefly described|p103 Fig.2. |Eocene|Eocene|||Unit in Nirranda Group.||Unconformably overlies Dilwyn Formation. Is overlain by Narrawaturk Marl.|Shallow to nearshore marine sandstone and shale.|
11654|Mepunga Formation|67367|5|Briefly described|p131 Fig.2. |Late Eocene|Middle Eocene|||Unit in Nirranda Group.||||
11654|Mepunga Formation|68116|5|Briefly described|Appendix, Maps 54-55.|Eocene|Eocene|Contains barrier island, beach and near shore, estuarine and lagoonal deposits.|||||Quartz sand: medium to coarse grained, iron-stained, minor detrital limonite, with gastropod and mollusc fragments; foraminifers; unconsolidated, locally cemented with calcite, interbedded with carbonaceous clayey silt to silty clay.|
11654|Mepunga Formation|69297|5|Briefly described|p79, p98|Bartonian|Bartonian|Otway Basin.||Nirranda Group||Unconformably overlies the Dilwyn Formation. Overlain by the Narrawaturk Marl.|Siltstone.|
11654|Mepunga Formation|69651|5|Briefly described|p10|Oligocene|Eocene|||Nirranda Group.||Unconformably overlies Dilwyn Formation. Is overlain by Narrawaturk Marl.||
11654|Mepunga Formation|70077|5|Briefly described|Nelson: Fig.2. Regional: Fig.4; p5|Eocene|Eocene|Otway Basin. Prograding nearshore to offshore marine clastics. Time-equivalent to Demons Bluff Formation and Eastern View Coal Measures.||Basal unit in Nirranda Group.||Overlies Dilwyn Formation. Is overlain by Narrawaturk Marl.||
11654|Mepunga Formation|70078|5|Briefly described|Northern: Fig.2. Regional: Fig.4|Eocene|Eocene|Gambier Embayment and Voluta Trough.||Nirranda Group.||Overlies Dilwyn Formation. Is overlain by Narrawaturk Marl.||
11654|Mepunga Formation|70193|6|Mentioned|p285 fig 3|||||||||
11654|Mepunga Formation|70880|6|Mentioned|p77|Oligocene|Eocene|Otway Basin.||||||
11654|Mepunga Formation|70942|4|Described|p126, 119|||||||||17-FEB-17
11654|Mepunga Formation|71266|6|Mentioned|p614 Fig.3|Oligocene|Eocene|Otway Basin.||||||
11654|Mepunga Formation|71437|4|Described|Fig. 1 opp 154, p155, p160|Eocene|Eocene|||Of Nirranda Group.||Sharp or transitional contact with [p155] Interfingers with  overlying Narrawaturk Marl [p160].|Mainly brown limonitic quartz sands, calcareous limonitic sands, and limonitic  sandy limestones, with some pyritic carbonaceous sandy mudstones.|
11654|Mepunga Formation|73357|5|Briefly described|p28-29, p31, p44, p46, p48|Priabonian|Bartonian|Otway Basin. Contains the Nothofagidites asperus Spore-Pollen Zone, non-marine to nearshore marine depositional environment. Correlated with Corrudinium incompositum Dinocyst Zone.||Of Nirranda Group||Overlies Dilwyn Formation, underlies Narrawaturk Marl.|Includes shales.|
11654|Mepunga Formation|73383|5|Briefly described|p3, p10 Tb.3.7, p21, p25, p165, p258|Eocene|Eocene|Otway Basin. Approximately equivalent to chemostratigraphic package S5-P10 which has high Si/Al and Th/Sc values. The top of the package is defined by an increase in Ca abundance into the overlying sequence. Lithologies based on geochemistry using the ChemLith classification includes calcareous and argillaceous sandstones, and using the Herron classification (1988) includes quartz arenite and Fe-sand. See also vi, p11 Tb.3.9, p34-35, p131, p137, p264.||Nirranda Group||Overlies Dilwyn Formation, Wangerrip Group, underlies Narrawaturk Marl|Very mature quartz-rich sandstone.|
11654|Mepunga Formation|73385|5|Briefly described|p5|Eocene|Eocene|Otway Basin.||Nirranda Group||Overlies Dilwyn Formation, underlies Narrawaturk Marl.|Shallow marine and nearshore sandstones.|
11654|Mepunga Formation|73386|4|Described|p4, p6, p13, Attachment A1|Priabonian|Bartonian|Otway Basin. Interpreted to comprise multiple transgressive sandstone units which step landwards in a north-westward direction, range of high energy siliciclastic shoreline to shelf facies. Shallow marine and nearshore depositional environments. Belongs to the Lower-Middle Nothofagidites asperus spore-pollen subzones.||Nirranda Group||Overlies Dilwyn Formation, Wangerrip Group, underlies Narrawaturk Marl|Sandstones and shales.|
11654|Mepunga Formation|73486|6|Mentioned|p511 Fig.2|Rupelian|Lutetian|Otway Basin.||Nirranda Group||||
11654|Mepunga Formation|73594|5|Briefly described|p4|Eocene|Eocene|Otway Basin.||Nirranda Group||Underlies Narrawaturk Marl|Shallow marine and nearshore sandstones.|
11667|Mereenie Sandstone|9199|5|Briefly described|Map legend|Devonian|Silurian|White cross-bedded sandstone.  Geological Province: Amadeus Basin.||||||
11667|Mereenie Sandstone|9814|5|Briefly described|Map Legend|Devonian|Devonian|White cross-bedded sandstone.||||||
11667|Mereenie Sandstone|12891|5|Briefly described|p733 Fig. 2|Early Devonian|Late Silurian|Geological province: Amadeus Basin.||||||07-FEB-11
11667|Mereenie Sandstone|22560|5|Briefly described|p3|||Age "mostly" Silurian,  Max and Min limits not specified||||||01-SEP-09
11667|Mereenie Sandstone|22561|4|Described|p22|Devonian|Early Cambrian|||||||
11667|Mereenie Sandstone|22564|4|Described|p60|||Age Siluro-Devonian.  Overlying unit - Pertnjara Group||||||
11667|Mereenie Sandstone|22565|5|Briefly described|p70 & Table 1||Silurian|Thickness at Areyonga Creek measured from surface expression - 700m thick.  Approx. thickness measured from seismic data 710m.||||||
11667|Mereenie Sandstone|22566|4|Described|p84|Early Devonian|Silurian|Of the Larapinta Group.||||||06-NOV-06
11667|Mereenie Sandstone|22646|5|Briefly described|p 107|Devonian|Silurian|Underlain by Harajica and Ooraminna Sandstones in different sections - p107.||||||06-NOV-06
11667|Mereenie Sandstone|22650|4|Described|p 163|Early Devonian||Age of base of Mereenie Sandstone is not known but may be as old as latest Ordovician.||||||
11667|Mereenie Sandstone|22651|6|Mentioned|Fig 10 btw p182-183|||Age Siluro-Devonian.||||||
11667|Mereenie Sandstone|22656|5|Briefly described|p 279|Devonian|Silurian|||||||
11667|Mereenie Sandstone|22760|4|Described|p337|Devonian||Origin - Aeolian Deposition.  Age - Siluro-Devonian.||||||
11667|Mereenie Sandstone|22761|4|Described|p349-350|Early Devonian|Late Ordovician|Age - Mostly Silurian.||||||06-NOV-06
11667|Mereenie Sandstone|22762|5|Briefly described|p369|Devonian|Silurian|||||||
11667|Mereenie Sandstone|22763|5|Briefly described|p394|Early Devonian|Silurian|||||||
11667|Mereenie Sandstone|22804|4|Described|p442|||Poorly constrained age but is generally assumed to be Silurian to Early Devonian.||||||06-NOV-06
11667|Mereenie Sandstone|22805|5|Briefly described|p465||Early Devonian|||||||
11667|Mereenie Sandstone|22806|6|Mentioned|Fig 6 on p481|||Age - Ordovician(?)-Devonian(?)||||||
11667|Mereenie Sandstone|22807|6|Mentioned|Fig 3 on p495|Devonian|Silurian|||||||
11667|Mereenie Sandstone|22824|5|Briefly described|p526|||||||||
11667|Mereenie Sandstone|22826|4|Described|p575|Early Devonian|Late Ordovician|||||||
11667|Mereenie Sandstone|23282|6|Mentioned|p83|||May correlate with Mimili Formation. In the Amadeus Basin.||||||06-NOV-06
11667|Mereenie Sandstone|23361|5|Briefly described|16 Fig.4|Early Devonian|Caradoc|Age: 450-400Ma.||||||06-NOV-06
11667|Mereenie Sandstone|23858|5|Briefly described|p914|Late Ordovician|Late Ordovician|Overlain by Pertnjara Group; underlain by Carmichael Sandstone. Geological Province: Amadeus Basin. Max. thickness: 1500 m.||||||06-NOV-06
11667|Mereenie Sandstone|24063|5|Briefly described|p220|Devonian|Silurian|Geological Province: Amadeus Basin. Maximum thicknes: >900m.||||||
11667|Mereenie Sandstone|24064|5|Briefly described|p229 Fig.7|Devonian|Silurian|Geological Province: Amadeus Basin.||||||
11667|Mereenie Sandstone|24111|5|Briefly described|p214 Fig. 9|Devonian|Devonian|Geological Province: Amadeus Basin.  See also p215 Fig. 11.||||||30-MAR-05
11667|Mereenie Sandstone|24301|5|Briefly described|p21|||Unconformably overlies Carmichael Sandstone.  Geological Province: Amadeus Basin||||||06-NOV-06
11667|Mereenie Sandstone|24334|4|Described|p43, p48 Tb.1|Early Devonian|Caradoc|Age: 391 - 458 Ma (?evidence for this precision?).  Overlies the Carmichael Sandstone.  Overlain by the Parke Siltstone.||||||01-SEP-09
11667|Mereenie Sandstone|29474|6|Mentioned|p10|||||||||
11667|Mereenie Sandstone|29591|5|Briefly described|Table 23|||||||||
11667|Mereenie Sandstone|29972|6|Mentioned|p5|||Silurian-Devonian||||||
11667|Mereenie Sandstone|30045|6|Mentioned|p343|||||||||
11667|Mereenie Sandstone|30075|6|Mentioned|p12|||||||||
11667|Mereenie Sandstone|30238|4|Described|p64|||Devonian age.||||||06-NOV-06
11667|Mereenie Sandstone|30544|5|Briefly described|p50|||See also p51.||||||06-NOV-06
11667|Mereenie Sandstone|30615|6|Mentioned|p177|||Stratigraphic table - Palm Valley -2||||||
11667|Mereenie Sandstone|30659|6|Mentioned|p89|||Devonian. Palaeomagnetism.||||||
11667|Mereenie Sandstone|30661|6|Mentioned|Table 1|||||||||
11667|Mereenie Sandstone|30662|6|Mentioned|p188|||Palaeomagnetic dates||||||
11667|Mereenie Sandstone|31566|5|Briefly described|p229|||? Silurian - Devonian. See also p230, 231, 233, 239 etc.||||||06-NOV-06
11667|Mereenie Sandstone|31707|6|Mentioned|Table 1|||See also Fig. 2||||||
11667|Mereenie Sandstone|31914|6|Mentioned|p97|||Equivalent? Lennis Sst. & of Wanna Beds.||||||
11667|Mereenie Sandstone|32208|6|Mentioned|Map legend|Devonian|Silurian|Silurian? and Devonian?||||||
11667|Mereenie Sandstone|32619|6|Mentioned|p465|||||||||
11667|Mereenie Sandstone|32648|6|Mentioned|p32|||Sil. - Dev.||||||
11667|Mereenie Sandstone|32865|6|Mentioned|p482|||Partly Dev.||||||
11667|Mereenie Sandstone|33307|6|Mentioned|Fig.6|||||||||
11667|Mereenie Sandstone|33326|6|Mentioned|p449|||||||||
11667|Mereenie Sandstone|33625|6|Mentioned|p185|||Table 2||||||
11667|Mereenie Sandstone|33761|6|Mentioned|p146|||Sil? - Dev.||||||
11667|Mereenie Sandstone|33832|6|Mentioned|p8|||Stratigraphy||||||
11667|Mereenie Sandstone|33844|6|Mentioned|Table 1|||||||||
11667|Mereenie Sandstone|33871|6|Mentioned|Fig.4|||||||||
11667|Mereenie Sandstone|33971|6|Mentioned|p34|||Lithology sim. to Crown Pt. Fm.||||||
11667|Mereenie Sandstone|34111|5|Briefly described|p12|||Silurian? - Devonian. See also pp14,16,18.||||||06-NOV-06
11667|Mereenie Sandstone|34433|6|Mentioned|p41|||||||||
11667|Mereenie Sandstone|34442|5|Briefly described|Table 1|||Silurian? - Devonian.||||||06-NOV-06
11667|Mereenie Sandstone|34579|4|Described|Table 2|||Silurian - Devonian. See also pp10,16,17.||||||06-NOV-06
11667|Mereenie Sandstone|35088|6|Mentioned|p98|||||||||
11667|Mereenie Sandstone|35102|6|Mentioned|Fig.2|||||||||
11667|Mereenie Sandstone|35223|6|Mentioned|p11|||||||||
11667|Mereenie Sandstone|35997|6|Mentioned|p577|||||||||
11667|Mereenie Sandstone|36473|6|Mentioned|Map legend|Carboniferous|Devonian|Between Carboniferous and Devonian||||||
11667|Mereenie Sandstone|36751|6|Mentioned|p489|||||||||
11667|Mereenie Sandstone|36821|6|Mentioned|p397|||||||||
11667|Mereenie Sandstone|36890|4|Described|p400|||Formerly Mareena Bluff Formation.||||||06-NOV-06
11667|Mereenie Sandstone|37727|4|Described|p72|||See also p14.||||||06-NOV-06
11667|Mereenie Sandstone|37818|6|Mentioned|p81|||||||||
11667|Mereenie Sandstone|38606|6|Mentioned|Map legend|Devonian|Devonian|||||||
11667|Mereenie Sandstone|38885|6|Mentioned|Map legend|Devonian|Devonian|||||||
11667|Mereenie Sandstone|39213|6|Mentioned|Fig.6|||Amadeus Basin Succession||||||
11667|Mereenie Sandstone|39565|6|Mentioned|Fig.14|||||||||
11667|Mereenie Sandstone|39583|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
11667|Mereenie Sandstone|40136|6|Mentioned|p36|||||||||
11667|Mereenie Sandstone|40201|5|Briefly described|Table 1|||||||||
11667|Mereenie Sandstone|40387|6|Mentioned|p146|||||||||
11667|Mereenie Sandstone|40642|6|Mentioned|p172|||||||||
11667|Mereenie Sandstone|40740|3|Fully described|p58|||Mention p6.||||||06-NOV-06
11667|Mereenie Sandstone|40810|5|Briefly described|p11|||||||||
11667|Mereenie Sandstone|40834|5|Briefly described|p138|||||||||
11667|Mereenie Sandstone|40906|6|Mentioned|p30|||Mention Fig.11||||||
11667|Mereenie Sandstone|40911|6|Mentioned|Map legend|Devonian|Devonian|Prob. Devonian||||||
11667|Mereenie Sandstone|40926|6|Mentioned|p12|||||||||
11667|Mereenie Sandstone|41018|6|Mentioned|p233|||||||||
11667|Mereenie Sandstone|41039|4|Described|p6|||||||||
11667|Mereenie Sandstone|41190|6|Mentioned|Fig.4|||||||||
11667|Mereenie Sandstone|41224|6|Mentioned|Fig.2|||||||||
11667|Mereenie Sandstone|41270|6|Mentioned|p270|||||||||
11667|Mereenie Sandstone|41276|6|Mentioned|p61|||||||||
11667|Mereenie Sandstone|41385|6|Mentioned|p363|||||||||
11667|Mereenie Sandstone|41409|6|Mentioned|p290|||||||||
11667|Mereenie Sandstone|41560|6|Mentioned|p551|||||||||
11667|Mereenie Sandstone|41621|5|Briefly described|Map legend|Middle Devonian|Late Ordovician|||||||
11667|Mereenie Sandstone|41717|6|Mentioned|Fig.2|||||||||
11667|Mereenie Sandstone|41723|6|Mentioned|Map legend|Late Ordovician|Early Devonian|||||||
11667|Mereenie Sandstone|41819|6|Mentioned|Map legend|Middle Devonian|Late Ordovician|||||||
11667|Mereenie Sandstone|41820|3|Fully described|p13|||||||||
11667|Mereenie Sandstone|42049|5|Briefly described|p217|||||||||
11667|Mereenie Sandstone|42058|6|Mentioned|p116|||||||||
11667|Mereenie Sandstone|42059|6|Mentioned|Fig.2 P131|||||||||
11667|Mereenie Sandstone|42060|6|Mentioned|Fig.5 P140|||||||||
11667|Mereenie Sandstone|42082|6|Mentioned|Fig.3 P323|||||||||
11667|Mereenie Sandstone|42140|6|Mentioned|p558|||||||||
11667|Mereenie Sandstone|42141|6|Mentioned|p568|||||||||
11667|Mereenie Sandstone|42504|5|Briefly described|p77|||||||||
11667|Mereenie Sandstone|42643|6|Mentioned|p32|||||||||
11667|Mereenie Sandstone|42699|5|Briefly described|map legend|Devonian|Silurian|||||||
11667|Mereenie Sandstone|42776|6|Mentioned|p305|||||||||
11667|Mereenie Sandstone|42940|5|Briefly described|Plate 2|Silurian|Silurian|Sandstone, minor conglomerate.  Age: 440-410Ma.  Geological province: Amadeus Basin.||||||23-JAN-08
11667|Mereenie Sandstone|43035|5|Briefly described|p23|||||||||
11667|Mereenie Sandstone|43105|5|Briefly described|Fig.3,p8.|||||||||
11667|Mereenie Sandstone|43225|5|Briefly described|Map Legend|Devonian|Ordovician|||||||
11667|Mereenie Sandstone|43503|6|Mentioned|11-39|Early Devonian|Silurian|||||||
11667|Mereenie Sandstone|43646|6|Mentioned|Fig.3,p554|Devonian|Silurian|||||||
11667|Mereenie Sandstone|43647|6|Mentioned|p530|||||||||
11667|Mereenie Sandstone|43648|5|Briefly described|Fig.1,p488|||||||||
11667|Mereenie Sandstone|43649|5|Briefly described|fig.1,p454-455,459|||||||||
11667|Mereenie Sandstone|43666|6|Mentioned|p20|||||||||
11667|Mereenie Sandstone|43749|6|Mentioned|p37|||||||||
11667|Mereenie Sandstone|43817|5|Briefly described|p61-63|||||||||
11667|Mereenie Sandstone|43869|5|Briefly described|p10|Silurian|Silurian|Wind-blown sand, very porous and stores large quatities of water; main source of groundwater for Alice Springs.  Deposited about 430my ago.||||||06-NOV-06
11667|Mereenie Sandstone|44133|4|Described|p42 Fig. 7.16, 44|Middle Paleozoic|Early Paleozoic|Geological Province: Amadeus Basin. Conformably underlies: Finke Group. May exceed 600m in Thickness in depressions. Conformably overlain by Polly Conglomerate, Langra Formation, Horseshoe Bend Shale.||||||07-NOV-08
11667|Mereenie Sandstone|44158|6|Mentioned|p33|||of Amadeus Basin.||||||
11667|Mereenie Sandstone|44220|14|Not recorded|p.67|||||||||
11667|Mereenie Sandstone|44335|4|Described|p.11|Devonian|Silurian|Table 2. p.10, Sil-Dev.||||||
11667|Mereenie Sandstone|44336|14|Not recorded|map legend|Devonian|Silurian|SG/53-3.  Silurian-Devonian.||||||
11667|Mereenie Sandstone|44342|6|Mentioned|p.5, Table 2|||SG/53-5. ?Silurian-Devonian.||||||
11667|Mereenie Sandstone|44343|14|Not recorded|map legend|Devonian|Silurian|Silurian-Devonian.||||||
11667|Mereenie Sandstone|44393|4|Described|p.3, Tb.1|||||||||
11667|Mereenie Sandstone|44394|14|Not recorded|map legend|||Silurian (?) to Devonian.||||||
11667|Mereenie Sandstone|44395|14|Not recorded|p.9,10,12, Tb.2||Late Ordovician|Upper Ordovician.||||||
11667|Mereenie Sandstone|44396|5|Briefly described|map legend|||(Sil?-Dev). SF/52-15.||||||
11667|Mereenie Sandstone|44402|5|Briefly described|map legend|||Silurian? - Dev.||||||02-DEC-04
11667|Mereenie Sandstone|44433|14|Not recorded|map legend|||Silurian? to Devonian.||||||
11667|Mereenie Sandstone|44439|2|Defined|p.7,8, Tb.1, map|Devonian|Ordovician|Ordovician-Devonian.||||||
11667|Mereenie Sandstone|44440|14|Not recorded|map legend|Devonian|Ordovician|Ordovician-Devonian.||||||
11667|Mereenie Sandstone|44484|14|Not recorded|p.5,8,9,11,Fig.4,Tb1|||(?Sil-Dev). See also p.11,12,14, for more details.||||||
11667|Mereenie Sandstone|44485|14|Not recorded|map legend|||Sil? - Dev.||||||
11667|Mereenie Sandstone|44493|4|Described|p.11, map|Devonian|Ordovician|Bloods Range sheet. (G53-3). Ord-Dev. See p.8,13, for details.||||||
11667|Mereenie Sandstone|44494|14|Not recorded|map legend|Devonian|Ordovician|Ordovician - Devonian.||||||
11667|Mereenie Sandstone|44495|4|Described|p.6, map|Devonian|Ordovician|See p.8-10, Tb.1, for details. (G52-8). Ord-Dev.||||||
11667|Mereenie Sandstone|44497|4|Described|p.11,12, Table 2|Devonian|Ordovician|SF/53-13. Ord-Dev.||||||
11667|Mereenie Sandstone|44498|14|Not recorded|map legend|Devonian|Ordovician|Ordovician-Devonian.||||||
11667|Mereenie Sandstone|44505|14|Not recorded|p.2,4,8,9,Fig 1,Tb.1|Devonian|Silurian|Sil-Dev. See also p.9,12, for more details.||||||
11667|Mereenie Sandstone|44506|14|Not recorded|map legend|||Silurian? to Devion.||||||
11667|Mereenie Sandstone|45036|6|Mentioned|p3|||||||||
11667|Mereenie Sandstone|45041|4|Described|p86|||See also pp87-89. U.Sil.- M.Dev.||||||06-NOV-06
11667|Mereenie Sandstone|45148|6|Mentioned|p20|||||||||
11667|Mereenie Sandstone|45155|6|Mentioned|Fig.8|||||||||
11667|Mereenie Sandstone|45168|6|Mentioned|p6|||||||||
11667|Mereenie Sandstone|45170|6|Mentioned|p8|||||||||
11667|Mereenie Sandstone|46829|6|Mentioned|Fig.2|||||||||
11667|Mereenie Sandstone|46928|6|Mentioned|Table 1|||||||||
11667|Mereenie Sandstone|47050|5|Briefly described|p240|||||||||
11667|Mereenie Sandstone|48639|4|Described|p.4|||See also p.1,5-7,16,Pl.1,Sh.1. ?Ord (Siln-Devn according to B.M.R.) F53-14,G55-2).||||||
11667|Mereenie Sandstone|48838|2|Defined|p.19,22-23, Tb.1|||||||||
11667|Mereenie Sandstone|48842|4|Described|p.20||Paleozoic|p.1,20,27,32,Pl.7. Tb.I.||||||07-NOV-08
11667|Mereenie Sandstone|48862|14|Not recorded|p.1,15,18,25,27-42|||(F52-15). Age uncertain, base at least is Ord. opp.8,9; Pl.4,5,9-11.||||||
11667|Mereenie Sandstone|48863|2|Defined|p.29|||Tb.1. opp.p.7,9,20,28,31,36,37-40,42,Pl.4,9,11,13-14,16. Ordovician-Devonian. (G52-4,G53-1).||||||
11667|Mereenie Sandstone|48864|2|Defined|p.34|Middle Devonian|Early Ordovician|Tb.1. On many pages. p.2,9,10,21,32,35,37,48,50,Pl.10,11,13. L.Ord-Lower or Middle Devonian. (G52-2,3,8).||||||
11667|Mereenie Sandstone|48865|2|Defined|p.4,Fig.26-27|||Many figures. Fig.4,21,25,42,47,51,Fig.14, Pl.8-10. = 'Marena red sandstone'. Upper Ordovician? (G52-8,G53-5).||||||06-NOV-06
11667|Mereenie Sandstone|48880|14|Not recorded|p.20,33,Pl.10,11,13|Devonian|Ordovician|(F53-13,14,G53-3).Ord-Devn.||||||
11667|Mereenie Sandstone|48890|4|Described|p.48, pl.12|Devonian|Silurian|See also Tables, Figs & Plates. Sil-Dev.||||||
11667|Mereenie Sandstone|48963|6|Mentioned|Fig.3|||||||||
11667|Mereenie Sandstone|50098|5|Briefly described|p1||Late Ordovician|Geological Province: Amadeus Basin.||||||
11667|Mereenie Sandstone|50244|6|Mentioned|p100|||||||||
11667|Mereenie Sandstone|60547|5|Briefly described|Map Legend|Devonian|Silurian|White cross-bedded sandstone. Geological Province: Amadeus Basin.||||||
11667|Mereenie Sandstone|60674|5|Briefly described|Map legend|Devonian|Silurian|Of the Pertnjara Group.  White to pale brown, fine, well-sorted quartz sandstone.  Geological Province: Amadeus Basin.||||||03-DEC-15
11667|Mereenie Sandstone|61306|5|Briefly described|p14, p40|||High-yielding aquifer rocks. Geological Province: northern Amadeus Basin||||||
11667|Mereenie Sandstone|61309|5|Briefly described|p16 Fig. 4, p25 Fig. 11|||Geological Province: Amadeus Basin.||||||06-FEB-08
11667|Mereenie Sandstone|61385|5|Briefly described|Map legend|Devonian|Silurian|White, crossbedded sandstone.  Geological Province: Amadeus Basin.||||||20-OCT-05
11667|Mereenie Sandstone|61387|5|Briefly described|Map legend|Devonian|Silurian|Of the Pertnjara Group. White sandstone, large-scale cross-bedding.  Geological Province: Amadeus Basin.||||||06-NOV-06
11667|Mereenie Sandstone|61518|5|Briefly described|Map Legend|Devonian|Silurian|White to pale brown fine grained, well sorted quartz sandstone. Geological Province: Amadeus Basin.||||||
11667|Mereenie Sandstone|61519|5|Briefly described|Map Legend|Silurian|Silurian|Of the Pertnjara Group. White sandstone, large scale cross bedding. Geological Province: Amadeus Basin.||||||
11667|Mereenie Sandstone|62359|6|Mentioned|p547 Fig. 7|||Geological Province: Amadeus Basin.||||||
11667|Mereenie Sandstone|62376|5|Briefly described|p18|Early Devonian|Silurian|Of the Larapinta Group. Geological Province: Amadeus Basin.||||||09-FEB-10
11667|Mereenie Sandstone|62379|5|Briefly described|p7 Fig. 2|Devonian|Silurian|Of the Larapinta Group. Geological Province: Amadeus Basin.||||||
11667|Mereenie Sandstone|62609|5|Briefly described|Map Legend|Devonian|Silurian|Sandstone, minor conglomerate. Underlies: Pertnjara Group. Overlies: Larapinta Group.||||||14-AUG-06
11667|Mereenie Sandstone|62620|5|Briefly described|Map Legend|Devonian|Silurian|Sandstone, minor  conglomerate.||||||
11667|Mereenie Sandstone|63562|5|Briefly described|p338 fig 3, p352 fig 10, p355|Devonian|Silurian|See also p347 fig 9, p350. Of Amadeus Basin. Up to 1.5 km thick package. Zircons similar to underlying sediments (mostly 0.63-0.49 Ga) thus presumed to be derived from them. Similar age spectrum as Stairway Sandstone.|c.435-405 Ma.|||Overlies Carmichael Sandstone conformably. Overlain by Pertnjara Group unconformably.|Aeolian, lesser fluvial, quartz arenites.|
11667|Mereenie Sandstone|64068|6|Mentioned|p78, 79, p7|Silurian|Silurian|Amadeus Basin. Correlated with Devonian Dulcie Sandstone, Cravens Peak beds, Georgina Basin.||||||
11667|Mereenie Sandstone|64334|5|Briefly described|p39, 42|Silurian|Silurian|Amadeus Basin. Deposition was probably in a foreland basin with highlands to the N.||||Unconformably overlies Carmichael Sandstone (Larapinta Group).|Aeolian, fluvial and locally marginal-marine deposits.|
11667|Mereenie Sandstone|64580|4|Described|map legend|Silurian|Ordovician|Quartz sandstone; minor siltstone; eolian.||||||09-DEC-08
11667|Mereenie Sandstone|64769|6|Mentioned|p29|||Dimension stone from this unit is called Ooraminna Sandstone.||||||06-MAY-09
11667|Mereenie Sandstone|64778|6|Mentioned|p13, 16-17, 20|Silurian|Silurian|Amadeus and Pedirka Basins. Max. palaeotemperature analysis summary.||||||
11667|Mereenie Sandstone|64809|5|Briefly described|p2, p3 Fig.2, p6 Fig.4, p11 Fig.10 |Early Devonian|Silurian|Aeolian and fluvial deposition.||||||
11667|Mereenie Sandstone|64970|6|Mentioned|p719 Fig. 2|Devonian|Silurian|Geological Province: Amadeus Basin.||||||27-MAY-09
11667|Mereenie Sandstone|65194|6|Mentioned|p30, p57, p59, p67|Paleozoic||Amadeus Basin. Misspelt as Meerenie on p67. Aquifer supplying Alice Springs.||||||
11667|Mereenie Sandstone|65233|4|Described|p3 Fig. 2, p10, p12-13|Early Devonian|Silurian|Of upper Larapinta Group. Gradational with Carmichael Sandstone below. Max.thickness:900m. Geol.prov: Amadeus Basin. Comprises 3 unnamed units - lower aeolian succession overlain by locally developed fluvial deposits, capped by an upper aeolian sandstone.||||||07-FEB-11
11667|Mereenie Sandstone|65272|6|Mentioned|p319, p320 Fig.3|Devonian|Silurian|||||||
11667|Mereenie Sandstone|65342|6|Mentioned|p3, p10.|||Amadeus and Eromanga Basins. Max. thickness at least 338 m.||||Overlies Stairway Sandstone. Is overlain by Pertnjara Group.||
11667|Mereenie Sandstone|65449|5|Briefly described|p34-35|Early Devonian|Late Ordovician|Amadeus Basin. Marginal marine to eolian deposits. Closely resembles Tandalgoo Formation lithologically.||||Time-correlative with Carribuddy Group and Worral Formation.||
11667|Mereenie Sandstone|65489|5|Briefly described|p56, p63-64, p125|Devonian|Devonian|Amadeus Basin. Exhibits particularly good reservoir properties at McDills 1.||||||
11667|Mereenie Sandstone|66767|5|Briefly described|p60|Devonian|Late Ordovician|Amadeus Basin. Up to 1000m thick.||||Overlies Larapinta Group. Is overlain unconformably by Pertnjara Group.|Shallow-marine to fluvial quartz sandstone.|
11667|Mereenie Sandstone|67028|6|Mentioned|p372 Tb. 5|Devonian|Ordovician|Magnetic information for unit concerning Mid-Paleozoic to Early Mesozoic pole positions for Australia is presented, sourced from the Global Palaeomagnetic Database (GPMDB; McElhinny & Lock 1993, 1996).|398-461 Ma magnetic age range|||||24-APR-12
11667|Mereenie Sandstone|67326|5|Briefly described|p2-3|Early Devonian|Silurian|Amadeus Basin.||Larapinta Group.||Overlies Carmichael Sandstone. Is overlain by Parke Siltstone.||
11667|Mereenie Sandstone|67565|5|Briefly described|p5 Fig.3, p42, p47, p52.|||Amadeus Basin. Widespread; occurs as prominent ridges. Shallow marine sands overlain  by aeolian dunes. Thickness from 220-1000 m. Devonian fish remains were recorded from its upper beds. An important aquifer.||||Overlies Carmichael Sandstone. Is overlain by Pertnjara Group.|White to pale brown, fine-grained, well-sorted quartz sandstone.|
11667|Mereenie Sandstone|67856|4|Described|p338 fig 4-30, p347 , 337, 346, 348|Early Devonian|Late Ordovician|Of Wells et al., 1964, 1970 etc. [Database says it is part of Pertnjara Group. This reference says there is unconformity between them] Type section West of Ellery Creek (NT). Shallow marine, eolian, fluviatile. Up to 100 m thick [p346, or 1000m p347]. 9 m exposed in WA.||||Overlies Carmichael Sandstone (unconformably).  Overlain gradationally in some parts and unconformably in others by Pertnjara Group (NT).|White to pale brown, cross-bedded pure quartz sandstone.|
11667|Mereenie Sandstone|68323|6|Mentioned|p4 Fig.2|Early Devonian|Early Devonian|Amadeus Basin.||Larapinta Group.||||
11667|Mereenie Sandstone|69438|3|Fully described|p23:2-5,7,21,32, 36-39, 46-48, 50, 55-57|Late Devonian|Silurian|Pritchard and Quinlan (1962); previously spelled as Mareenie Sandstone (Madigan, 1932). Originally Mereenie Bluff Formation of Chewings (1894) for sandstone at the George Gill Range, Amadeus Basin. Was formerly mapped (Ranford et al., 1965) as including rocks which were subsequently (Wells et al., 1970) assigned as a separate Formation (the Carmichael Sandstone). The type section is in the west MacDonnell Ranges, W of Ellery Creek; reference sections at Stokes Pass and Areyonga Creek further to the W. Up to c.1000m thick. Widespread unit: extends c.800km E-W and c.200km N-S. Is faulted against Carnegie Formation. Is overlain by Brewer Conglomerate unconformably. Age range of Late Ordovician?-Early Devonian? is due to absence of useful fossils. Has been quarried for dimension stone in the Ooraminna area.||Ungrouped.||Overlies Carmichael Sandstone conformably (unconformably in the E), and Pertaoorrta Group unconformably. Is overlain by Parke Siltstone or Hermannsburg Sandstone conformably.|Variably thinly to thickly bedded, white to pale brown very pure quartz sandstone; generally fine-grained, but is occasionally medium-grained, with grains well-rounded and well-sorted. Burrows and arthropod tracks occur.|27-APR-17
11667|Mereenie Sandstone|69439|5|Briefly described|p24:11|Silurian|Ordovician|Amadeus Basin. Possible correlative of Kerridy Sandstone (Ngalia Basin).||||||12-JUL-16
11667|Mereenie Sandstone|69449|5|Briefly described|p34:2 Fig.34.2; 34:5, 7|Devonian|Silurian|Eastern Amadeus Basin, with equivalents in the western Warburton Basin. Potential petroleum reservoir rocks.||||Is overlain by Polly Conglomerate (Finke Group).|Red-brown to orange, fine- to coarse-grained, friable sandstone, cross-bedded and locally calcareous.|12-JUL-16
11667|Mereenie Sandstone|69458|6|Mentioned|p42:8|Early Devonian|Late Ordovician|Amadeus Basin.||||||12-JUL-16
11667|Mereenie Sandstone|69606|5|Briefly described|p3, p4 fig 2|Devonian|Silurian|One outcrop found in WA. Deposited during the Alice Springs Orogeny. Amadeus Basin. Potential reservoir rock.||||Unconformably overlies the Carmichael Sandstone. Unconformably overlain by the Pertnjara Group.|Sandstone.|
11667|Mereenie Sandstone|69673|5|Briefly described|p64 fig 53, p67, p149, p149 fig 120|||1km thick.||||Overlies Carmichael Sandstone, overlain by Parke Siltstone|Fine grained, occasionally medium grained, very pure quartz sandstone.|
11667|Mereenie Sandstone|69982|6|Mentioned|p42|Devonian|Late Ordovician|Amadeus Basin.||||||
11667|Mereenie Sandstone|70793|4|Described|500k_interpgeop14_lut.csv|Early Devonian|Silurian|Of Amadeus Basin (Phase 2). Events: Alice Springs Orogeny (450-295 Ma); Rodingan Movement (Alice Springs Orogeny phase 1) (450-420 Ma). See 500k_interpgeop14_lut.csv, 2_5m_interpgeop15_lut.csv.|443.4-393.3 Ma (inferred)||||Quartz sandstone; minor siltstone; largely eolian|
11667|Mereenie Sandstone|70826|6|Mentioned|p7 tbl 3|Devonian|Silurian|Amadeus Basin.||||||24-APR-20
11667|Mereenie Sandstone|71080|6|Mentioned|p30 fig 21|Devonian|Silurian|Amadeus Basin.|||||Dominantly sandstone.|
11667|Mereenie Sandstone|71146|5|Briefly described|p6, p28|Pragian|Ludlow|Amadeus Basin. Hosts trace fossils including burrows, trails, scratch marks and tunnels similar to those found in the Tumblagooda Sandstone.||||Overlies the Carmichael Sandstone (Larapinta Group).|Sandstone.|
11667|Mereenie Sandstone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||conglomerate, sandstone|
11667|Mereenie Sandstone|71268|4|Described|GEOL_LUT_CSV files|Early Devonian|Silurian|Geological province: Paterson Orogen. Of Bentley Basin. Events: Rodingan Movement (Alice Springs Orogeny phase 1) (450-420 Ma). See 1m_geologyp12_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv.|443.4-393.3 Ma (inferred)|Unit of Pertnjara Group.|||Porous, white to pale-brown, fine grained, well sorted quartz sandstone, minor conglomerate|
11667|Mereenie Sandstone|71279|5|Briefly described|p355 Fig.2,p360,p363-365,p374,p382 Tb.1|Early Devonian|Silurian|Amadeus Basin. Crops out in the Waterhouse Range. Magnetisation described. Modelled magnetic properties.||Larapinta Group.||||
11667|Mereenie Sandstone|71342|6|Mentioned|Ch9 p16, Ch9 p20|||||||Unconformably overlies the Stairway Sandstone. Unconformably overlain by the Finke Group.||
11667|Mereenie Sandstone|71618|6|Mentioned|p130|Devonian|Silurian|Of Amadeus Basin.||||||
11667|Mereenie Sandstone|72034|5|Briefly described|500k_interpgeop16_lut|Early Devonian|Silurian|Amadeus Basin (Phase 2).|||||Quartz sandstone; minor siltstone; largely eolian.|
11667|Mereenie Sandstone|72360|5|Briefly described|Map legend|Silurian|Silurian|Of Amadeus Basin.|||||White sandstone, large scale cross bedding.|09-SEP-19
11667|Mereenie Sandstone|72369|4|Described|iii,p3-4-4,34-35,37-40|||Of Amadeus Basin. Widespread in the Amadeus Basin, covering ~800 km east-west and 200 km north-south (Owen in Kennard et al 1986). No previous geochronological analysis, but inferred age constraints provided by c. 480 MA MDA of underlying mereenie Sandstone (Maidment 2005), and paleomagnetic investigation by Li et al. (1991), providing possible Silurian age. LA-ICP-MS U-Pb detrital zircon dating of sample HB15VJN091 (medium-grained quartz arenite) yielded an interpreted maximum depositional age of 486+\-5 Ma (youngest concordant zircon). This age is within certainty of that provided by Maidment 2005, but inconsistent with paleomagnetic age of Li et al. (1991). Contains Meso- to Neoproterozoic detrital zircon age populations (c. 1235-915 Ma) likely sourced from Musgrave Province. Late Neoproterozoic to Cambrian (c. 750-485 Ma) zircons may have been derived from distal greater Gondwanan input, as there are no known Cambrian sources proximal to Amadeus Basin. Archean-Paleoproterozoic grains (c. 3125-1840 Ma) may have been recycled from North Australian Craton. Sample locality, zircon description, SHRIMP results and analyses are discussed.||Unit of Larapinta Group.||Overlain by parke Siltstone, or disconformably by Hermannsburg Sandstone. Underlain by Carmichael Sandstone.|Variably thinly- to thickly bedded, white to pale brown, quartz sandstone.|18-DEC-19
11667|Mereenie Sandstone|72374|4|Described|iii,p3-4,20-24,26|||Of Amadeus Basin. Depositional environment: shallow marine in the lower part, becoming aeolian in upper. Paleomagnetic investigation by Li et al 1991 suggested a Silurian (444-419 Ma) age. Provenance studies by Normington et al 2018 indicate recycling of detritus from underlying Amadeus Basin succession, as well as primary sources including Musgrave Province. Sample HB16ND358 (sandstone) yielded an interpreted maximum depositional age of 505+\-5 Ma. Zircons of c. 1300-800 Ma (c. 1209, 1158, 1183 and 1127 Ma peaks) likely derived from Musgrave Province either directly, or recycled from underlying Amadeus Basin succession. Lesser groupings of c. 700-500 Ma and c. 2050-1450 Ma likely sourced directly from Aileron, Warumpi and Musgrave provinces, or recycled from underlying Amadeus Basin succession.||Publication layout suggests this is a unit of Larapinta Group.|||Variably thinly- to thickly bedded, white to pale brown sandstone; well-rounded and well-sorted, fine- to medium-grained quartz arenite.|11-OCT-19
11667|Mereenie Sandstone|72476|6|Mentioned|p36 Fig.9|||Amadeus Basin. Time-temperature thermal history diagram.||||||
11667|Mereenie Sandstone|73085|6|Mentioned|p1, p4|early Devonian|Silurian|||Larapinta Group||Underlain by Carmichael Sandstone. Overlain by Parke Siltstone (Pertnjara Group).||
11667|Mereenie Sandstone|73119|5|Briefly described|piii, p1, p21-23, Appendix|Silurian|Silurian[?]|Amadeus Basin, widespread. Depositional environment ranges from shallow marine to fluvial to aeolian. Geochron is new SHRIMP U-Pb detrital zircon maximum depositional age, which is younger than the previous youngest age of 486 +/- 5 Ma (Normington et al., 2018), although still older than the Silurian age proposed using palaeomagnetism (Li et al., 1991). Detrital zircon age components are dominated by Palaeozoic to Neoproterozoic and early Mesoproterozoic zircons with only a small number of older Proterozoic-Archean grains. Sourced dominantly from the Musgrave Province with contributions probably from reworked underlying strata originally sourced from the Aileron and Warumpi provinces. [See article for provenance discussion].|473 +/- 7 Ma SHRIMP U-Pb||||Includes poorly-sorted, medium-grained sandstone.|
11667|Mereenie Sandstone|73279|5|Briefly described|p3, p14|Devonian|Ordovician|Amadeus Basin. Detrital zircons analysed for Hf isotopic composition [see article].||||Underlain by Larapinta Group [Carmichael Sandstone]. Overlain by Pertnjara Group.|Includes sandstone.|
11667|Mereenie Sandstone|73281|6|Mentioned|Appendix (DIP)|||See DIP034_Petroleumdata.xlsx and DIP034_Welldata.xlsx.||||||
11702|Merreti Member|22773|5|Briefly described|Fig24.5p350|Early Cretaceous|Early Cretaceous|||||||
11702|Merreti Member|22799|3|Fully described|p20|Aptian|Aptian|Monash Formation||||||
11702|Merreti Member|22857|5|Briefly described|p548 App.1 Tb.A1.12|Albian|Aptian|Of the Monash Formation. Mudstone, siltstone, minor sandstone. Max. thickness: >120m. Geological Province: Berri Basin. See also p350 Fig.24.5.||||||
11702|Merreti Member|22887|4|Described|Table 5 p31|Early Cretaceous|Early Cretaceous|See also Fig.5 p12. Renmark Trough.||||||
11702|Merreti Member|22893|5|Briefly described|table5 fig4||Early Cretaceous|||||||
11702|Merreti Member|23836|5|Briefly described|p93|Cretaceous|Cretaceous|Of Monash Formation. Geological Province: Murray Basin.||||||
11702|Merreti Member|24551|6|Mentioned|p270|||Of the Monash Formation||||||
11702|Merreti Member|33488|2|Defined|p9|Early Cretaceous|Early Cretaceous|See also P10||||||
11702|Merreti Member|33490|4|Described|p10|||Aptian. See also P24||||||
11702|Merreti Member|35232|6|Mentioned|Table 2|||||||||
11702|Merreti Member|39211|6|Mentioned|p38|||Fig.23||||||
11702|Merreti Member|42966|1|Redefined|Table 7 p67|Aptian||of Monash Formation||||||
11702|Merreti Member|43218|4|Described|Fig.3 p22,p27|Albian|Aptian|Of Monash Formation||||||
11702|Merreti Member|44133|5|Briefly described|p127|Cretaceous|Cretaceous|Of the Monash Formation.||||||
11702|Merreti Member|44191|5|Briefly described|Map Legend||Early Cretaceous|||||||
11702|Merreti Member|49038|5|Briefly described|p23|||||||||
11702|Merreti Member|49040|6|Mentioned|p8|||||||||
11702|Merreti Member|61314|5|Briefly described|p123, p129|Aptian|Aptian|Middle part of the Monash Formation. A marine sequence of rocks - of marine mudstone, siltstone and minor sandstone. Overlies the Pyap Member; overlain by the Coombool Member. Geological Province: western Murray Basin.||||||
11702|Merreti Member|73228|5|Briefly described|p50-54|Early Cretaceous|Early Cretaceous|Berri Basin. Shallow marine depositional environment; deposited during peak marine transgression into the Berri Basin via the Eromanga Basin. Identified in Cooltong 1, Berri North 1, Nadda 1, Loxton 1, and Overland Corner 1 drillholes. Distribution is more widespread than Pyap Member, overlapping older sediments and intervening basement ridges.||Monash Formation.||Underlain by Pyap Member. Overlain by Coomool Member and Renmark Group.|Transgressive claystone and siltstone with glauconite, pyrite, carbonaceous fragments, mica and clay intraclasts; sandy in places.|01-NOV-22
11702|Merreti Member|73229|5|Briefly described|p66-68, p70-72, p74-75|Early Cretaceous|Early Cretaceous|Berri Basin. [Analysed using pXRF; see article].||Monash Formation.|||Transgressive claystone and siltstone with glauconite, pyrite, carbonaceous fragments, mica and clay intraclasts, sandy in places.|01-NOV-22
11718|Merrimelia Formation|13497|3|Fully described|iv, v, vi, viii, x, xi|Asselian|Stephanian|Cooper Basin. Name is derived from the local aboriginal word Merrimelia (Martin 1967b). A type section in core is mentioned and a sedimentary facies log of this type core is given on p76. Outcrop characteristics discussed briefly. Deposited in a glacial environment. Has poor oil source quality and richness. See also xii, xiii, p47-p48, p54, p61, p64-p67, p69 fig 6.1, p70, p75-p84, p86-p89, p119, p122, p131, p132 tbl 8.1, p138, p139 fig 8.18, p141, p146, p152 fig 9.25, p153, p157-p159, p173, p184, p190, p216.||Gidgealpa Group||Interfingers with and is overlain by the Tirrawarra Sandstone. Unconformably overlain by the Patchawarra Formation.|Conglomerate, diamictite, sandstone, conglomeratic mudstone, siltstone and shale.|
11718|Merrimelia Formation|13516|6|Mentioned|p147, fig 5|Early Permian|Early Permian|From Cooper Basin||||||
11718|Merrimelia Formation|22527|6|Mentioned|p 3, Fig 3|||||||||
11718|Merrimelia Formation|22839|6|Mentioned|P33|||||||||
11718|Merrimelia Formation|22883|6|Mentioned|P29|||Overlying unit is Tirrawarra Sandstone||||||
11718|Merrimelia Formation|23154|5|Briefly described|Map Legend|Early Permian||Geological Province - Cooper Basin.  Of the Gidgealpa Group.  Max age ? Late Carboniferous.||||||06-NOV-06
11718|Merrimelia Formation|23155|4|Described|p14|Early Permian|Late Carboniferous|Unit forms the base of the Gidgealpa Group.  Sparse spore pollen assemblages suggest a Late Carboniferous to Early Permian age.  Overlying unit on STRZELECKI - Tirrawarra Sandstone.||||||
11718|Merrimelia Formation|23375|4|Described|Fig2 p265,285||Asselian|In the Cooper Basin.||||||06-NOV-06
11718|Merrimelia Formation|23818|5|Briefly described|p123 Fig.54, p128|Sakmarian|Sakmarian|Geological Province: Cooper Basin. Max. thickness: 1190 ft.||||||
11718|Merrimelia Formation|23830|5|Briefly described|Fig. 3a|Permian|Carboniferous|Geological Province: eastern Arckaringa Basin and Cooper Basin.||||||12-SEP-05
11718|Merrimelia Formation|23832|4|Described|p327|Permian|Permian|Geological Province: Cooper Basin.||||||
11718|Merrimelia Formation|24210|5|Briefly described|p133 Fig. 2|Late Carboniferous|Late Carboniferous|Of the Gidgealpa Group. Glacial deposits. Geological Province: Cooper Basin. See also p132.||||||14-APR-08
11718|Merrimelia Formation|24212|5|Briefly described|p67 Fig. 3p|Early Permian|Early Permian|Age: >290Ma.  Geological Province: Cooper Basin.||||||
11718|Merrimelia Formation|29387|6|Mentioned|Table 2|||Refers to Gatehouse(1972).||||||
11718|Merrimelia Formation|29391|6|Mentioned|Table 5|||See p23.||||||22-AUG-18
11718|Merrimelia Formation|29393|6|Mentioned|Table 3|||Lower Permian.||||||
11718|Merrimelia Formation|29497|6|Mentioned|p31|||||||||
11718|Merrimelia Formation|29516|6|Mentioned|p25|||||||||
11718|Merrimelia Formation|30340|6|Mentioned|p2517|||Lithology||||||
11718|Merrimelia Formation|30341|5|Briefly described|p122|||Permian age.||||||06-NOV-06
11718|Merrimelia Formation|30540|6|Mentioned|Fig.6|||||||||
11718|Merrimelia Formation|30804|6|Mentioned|p10|||On Table 1.||||||
11718|Merrimelia Formation|30825|6|Mentioned|p37|||||||||
11718|Merrimelia Formation|30856|4|Described|Table 2|||Lower Permian age. See also p9.||||||06-NOV-06
11718|Merrimelia Formation|30857|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
11718|Merrimelia Formation|30873|5|Briefly described|p15|||||||||
11718|Merrimelia Formation|30921|6|Mentioned|Map legend|Artinskian|Sakmarian|Sakmarian - Artinskian||||||
11718|Merrimelia Formation|31145|5|Briefly described|Table 1|||Lower Permian||||||
11718|Merrimelia Formation|31250|6|Mentioned|p8|||Microflora||||||
11718|Merrimelia Formation|31431|5|Briefly described|Table 2|||L.Permian||||||
11718|Merrimelia Formation|31436|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
11718|Merrimelia Formation|31591|6|Mentioned|p54|||See also p56, 57.||||||22-AUG-18
11718|Merrimelia Formation|31923|6|Mentioned|p12|||||||||
11718|Merrimelia Formation|32696|6|Mentioned|Fig.4|||See also Figs 6 & 7||||||
11718|Merrimelia Formation|33067|4|Described|Table 1|Permian|Permian|Sandstone, siltstone, coal, conglomerate.||||||07-JUL-04
11718|Merrimelia Formation|33074|5|Briefly described|p260|||||||||
11718|Merrimelia Formation|33078|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
11718|Merrimelia Formation|33079|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
11718|Merrimelia Formation|33082|6|Mentioned|Map legend|Permian|Permian|||||||
11718|Merrimelia Formation|33089|5|Briefly described|Table 2|||Permian||||||
11718|Merrimelia Formation|33331|6|Mentioned|p38|||||||||
11718|Merrimelia Formation|33489|6|Mentioned|Fig.2|||Refers Kapel (1972) & Gatehouse (1972)||||||
11718|Merrimelia Formation|33523|6|Mentioned|p23|||||||||
11718|Merrimelia Formation|33827|6|Mentioned|Table 2|||||||||
11718|Merrimelia Formation|33844|6|Mentioned|p56|||Refers Martin (1967)||||||
11718|Merrimelia Formation|33936|6|Mentioned|Fig.3A|||||||||
11718|Merrimelia Formation|33971|6|Mentioned|p34|||Lithology similar to Crown Pt. Fm.||||||
11718|Merrimelia Formation|33976|6|Mentioned|Fig.5|||||||||
11718|Merrimelia Formation|33977|5|Briefly described|p7|||Strat. Refers Martin (1967).||||||
11718|Merrimelia Formation|33998|6|Mentioned|p28|||||||||
11718|Merrimelia Formation|34065|6|Mentioned|p9|||L.Perm.||||||
11718|Merrimelia Formation|34218|6|Mentioned|p9|||Lower Permian||||||
11718|Merrimelia Formation|34309|6|Mentioned|p42|||Permian||||||
11718|Merrimelia Formation|34415|6|Mentioned|p79|||Lower Permian. See also pp80,81,82 etc.||||||22-AUG-18
11718|Merrimelia Formation|34487|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
11718|Merrimelia Formation|34612|4|Described|p128|||Permian. Sub-surface only.||||||
11718|Merrimelia Formation|34839|6|Mentioned|Fig.2|||||||||
11718|Merrimelia Formation|35067|6|Mentioned|Fig.4|||||||||
11718|Merrimelia Formation|35068|6|Mentioned|p52|||See also Fig.3||||||
11718|Merrimelia Formation|35279|6|Mentioned|Fig.5|||||||||
11718|Merrimelia Formation|35457|6|Mentioned|Fig.4|||Biostratigraphic relationships||||||
11718|Merrimelia Formation|35573|6|Mentioned|Fig.7|||Generalised stratigraphy - Southern Cooper Basin||||||
11718|Merrimelia Formation|35615|6|Mentioned|p1146|||||||||
11718|Merrimelia Formation|35845|4|Described|p23|||Lithology and depositional environments.||||||
11718|Merrimelia Formation|36099|6|Mentioned|Fig.2|||||||||
11718|Merrimelia Formation|36596|6|Mentioned|Text Fig.2|||||||||
11718|Merrimelia Formation|36910|6|Mentioned|p61|||||||||
11718|Merrimelia Formation|36917|6|Mentioned|Fig.1|||||||||
11718|Merrimelia Formation|37065|6|Mentioned|p32|||||||||
11718|Merrimelia Formation|37287|6|Mentioned|p36|||||||||
11718|Merrimelia Formation|37565|6|Mentioned|Fig.8|||||||||
11718|Merrimelia Formation|37855|6|Mentioned|p4|||See also Fig.2||||||
11718|Merrimelia Formation|37917|4|Described|p470|||||||||
11718|Merrimelia Formation|37926|6|Mentioned|p500|||||||||
11718|Merrimelia Formation|38068|5|Briefly described|p70|||||||||
11718|Merrimelia Formation|38226|6|Mentioned|Table 1|||||||||
11718|Merrimelia Formation|38779|6|Mentioned|p7|||||||||
11718|Merrimelia Formation|38977|6|Mentioned|p1423|||||||||
11718|Merrimelia Formation|39254|4|Described|p45|||||||||
11718|Merrimelia Formation|39261|6|Mentioned|Fig. 9|||||||||
11718|Merrimelia Formation|39264|6|Mentioned|Fig. 13|||||||||
11718|Merrimelia Formation|39265|6|Mentioned|Fig. 3|||||||||
11718|Merrimelia Formation|39276|6|Mentioned|Fig. 2|||||||||
11718|Merrimelia Formation|39445|5|Briefly described|Table 7|||||||||
11718|Merrimelia Formation|39478|6|Mentioned|Table 1|||||||||
11718|Merrimelia Formation|39494|6|Mentioned|Fig.3|||||||||
11718|Merrimelia Formation|39904|6|Mentioned|p14|||||||||
11718|Merrimelia Formation|40003|6|Mentioned|Fig.9|||||||||
11718|Merrimelia Formation|40030|6|Mentioned|Fig.3|||||||||
11718|Merrimelia Formation|40249|6|Mentioned|p45|||||||||
11718|Merrimelia Formation|40544|6|Mentioned|Fig.4|||||||||
11718|Merrimelia Formation|40637|6|Mentioned|Fig.2|||||||||
11718|Merrimelia Formation|40675|6|Mentioned|Table 12D|||||||||
11718|Merrimelia Formation|41097|6|Mentioned|p165|||||||||
11718|Merrimelia Formation|41099|6|Mentioned|p185|||||||||
11718|Merrimelia Formation|41131|6|Mentioned|Fig.3|||||||||
11718|Merrimelia Formation|41164|6|Mentioned|p422|||||||||
11718|Merrimelia Formation|41166|4|Described|p379|||||||||
11718|Merrimelia Formation|41183|6|Mentioned|Fig.3 p308|||||||||
11718|Merrimelia Formation|41198|6|Mentioned|Table 1|||||||||
11718|Merrimelia Formation|41214|6|Mentioned|Fig.3|||||||||
11718|Merrimelia Formation|41247|6|Mentioned|Fig.5|||||||||
11718|Merrimelia Formation|41267|6|Mentioned|Fig.2|||||||||
11718|Merrimelia Formation|41288|6|Mentioned|Fig.12|||||||||
11718|Merrimelia Formation|41491|6|Mentioned|Fig.8|||||||||
11718|Merrimelia Formation|41595|6|Mentioned|Fig. 4|||||||||
11718|Merrimelia Formation|41689|6|Mentioned|Table 1|||||||||
11718|Merrimelia Formation|41707|6|Mentioned|Fig.8|||||||||
11718|Merrimelia Formation|42042|6|Mentioned|p244|||||||||
11718|Merrimelia Formation|42062|6|Mentioned|p26|||||||||
11718|Merrimelia Formation|42067|4|Described|Appendix 2|||See also Fig.2 p309.||||||06-NOV-06
11718|Merrimelia Formation|42357|5|Briefly described|p4|||||||||
11718|Merrimelia Formation|42395|6|Mentioned|p79|||||||||
11718|Merrimelia Formation|42547|4|Described|p80|||||||||
11718|Merrimelia Formation|42746|5|Briefly described|p3, Fig.2 p4|||In the Cooper Basin.||||||06-NOV-06
11718|Merrimelia Formation|42966|6|Mentioned|p63|||||||||
11718|Merrimelia Formation|42999|5|Briefly described|Table 2,p90||Early Permian|||||||
11718|Merrimelia Formation|43002|5|Briefly described|Fig.2,p135|||||||||
11718|Merrimelia Formation|43004|5|Briefly described|Table 1,p179|||||||||
11718|Merrimelia Formation|43052|5|Briefly described|Table 2.1|||||||||
11718|Merrimelia Formation|43105|5|Briefly described|p14|||||||||
11718|Merrimelia Formation|43218|6|Mentioned|p26|||Cooper Basin. Correlated with Urana Formation, Murray Basin.||||||
11718|Merrimelia Formation|43570|5|Briefly described|Fig.2,p535,541|Early Permian|Late Carboniferous|||||||
11718|Merrimelia Formation|43628|6|Mentioned|Fig.3||Early Permian|||||||
11718|Merrimelia Formation|43841|6|Mentioned|7|||In Cooper Basin||||||
11718|Merrimelia Formation|44020|14|Not recorded|p9,10,13,Tb.1,2||Early Permian|||||||
11718|Merrimelia Formation|44133|5|Briefly described|p65 Fig 8.4, 82|Permian|Carboniferous|Of the Gidgealpa Group. Geological Province: Cooper Basin. Thickness: >290m.||||||
11718|Merrimelia Formation|45104|6|Mentioned|p30|||||||||
11718|Merrimelia Formation|46849|6|Mentioned|Fig. 7|||||||||
11718|Merrimelia Formation|48995|6|Mentioned|Fig.3|||||||||
11718|Merrimelia Formation|60386|6|Mentioned|p296|Sakmarian|Asselian|Cooper Basin. Non-marine.||||||
11718|Merrimelia Formation|60717|5|Briefly described|p40, p41|Late Carboniferous|Late Carboniferous|Of the Gidgealpa Group. Overlain by Tirrawarra Sandstone. Thickness: 450m. Geological Province: Cooper Basin. Glacial, lacustrine, aeolian deposits. See also Figure 2.||||||14-APR-08
11718|Merrimelia Formation|61614|6|Mentioned|p290 Fig. 2|Early Permian|Late Carboniferous|Of Gidgealpa Group. Geological Province: Cooper Basin.||||||17-MAR-09
11718|Merrimelia Formation|61615|5|Briefly described|p302, p303, p302 Fig. 2|Early Permian|Late Carboniferous|Of Gidgealpa Group. Geological Province: Cooper Basin. Glacial deposits.||||||07-FEB-11
11718|Merrimelia Formation|61616|6|Mentioned|p330 Fig. 2|Early Permian|Late Carboniferous|Of Gidgealpa Group. Geological Province: Cooper Basin.||||||
11718|Merrimelia Formation|61617|6|Mentioned|p343|Permian|Permian|Geological Province: Cooper Basin.||||||
11718|Merrimelia Formation|62046|5|Briefly described|p125 Fig. 2|Carboniferous|Carboniferous|Geological Province: Cooper-Eromanga Basins.||||||14-APR-08
11718|Merrimelia Formation|62537|6|Mentioned|p191 Fig.2, p192 .|Early Permian|Late Carboniferous|Cooper Basin. The basal sediments of the Merrimelia Formation were deposited around 295-305 Ma and uncomformably overlie the Warburton Basin.||Unit in Gidgealpa Group.||Is overlain by Tirrawarra Sandstone.||22-AUG-18
11718|Merrimelia Formation|62730|5|Briefly described|p352 Fig. 1|Late Carboniferous|Late Carboniferous|Geological Province: Cooper Basin.||||||14-APR-08
11718|Merrimelia Formation|63832|5|Briefly described|p131 Fig.2, p135|Cisuralian|Cisuralian|Cooper Basin. Is mentioned on p135 as the abbreviated [and mis-spelt] Tirrawarra-Merimelia Formations. Thick succession of continental proglacial and possibly subglacial facies.||||Is overlain by and interfingers with Tirrawarra Sandstone.|Continental proglacial and possibly subglacial facies.|13-DEC-17
11718|Merrimelia Formation|63978|2|Defined|p8, p9-10, Fig. 3|Early Permian|Early Permian|Of Gidgealpa Group. Intertongues with Tirrawarra Sandstone (mapped tog.as one 'unit'  in Fig. 13). Max.thick: 84m. Conglomerate, diamictite, sandstone, conglomeratic mudstone, siltstone + shale, commonly green-grey. Geol.prov: base of Cooper Basin.||||||07-FEB-11
11718|Merrimelia Formation|64048|5|Briefly described|p64 Tb. 2|||Geological Province: Cooper Basin. Oil reservoir at Malgoona.||||||07-FEB-11
11718|Merrimelia Formation|64197|6|Mentioned|p625 Fig.1c, p630 Fig.7|Early Permian|Late Carboniferous|Cooper Basin.||||Underlies Tirrawarra Sandstone and Patchawarra Formation.||11-DEC-15
11718|Merrimelia Formation|64631|5|Briefly described|p49.|Sakmarian|Asselian|Cooper Basin. Contains thick successions of continental proglacial facies. See also p44. Some biostratigraphic age control. Shown with time transgressive top boundary.||||Overlain by Tirrawarra Sandstone.||
11718|Merrimelia Formation|64665|5|Briefly described|p53 Fig.2, p56.|Early Permian|Early Permian|Cooper Basin. Hydrocarbon reservoirs are thought to have been charged from Patchawarra Formation.||||Is overlain by Tirrawarra Sandstone.||
11718|Merrimelia Formation|65489|5|Briefly described|p16, p48-49, p55, p96, p131-132, p143|Asselian|Late Carboniferous|Cooper Basin. 450m thick. Oil reservoir accounting for 1% of the Basin's production.||Basal unit in Gidgealpa Group.||Is overlain by Tirrawarra Sandstone and Patchawarra Formation. Equivalent to Crown Point Formation.|Terminoglacial and glaciofluvial systems including aeolianite.|
11718|Merrimelia Formation|65925|5|Briefly described|Appendix 2.||||||||Conglomerates, sandstone, glacigene lacustrine rhythmites.|
11718|Merrimelia Formation|67402|5|Briefly described|p90, p90 fig CPR4|||Deposited in glacio-fluvial environments. See also p91 tbl CPR1, p91, p92, p94, p101, p101 tbl CPR2.||Gidgealpa Group||Overlain by the Tirrawarra Sandstone and Patchawarra Formation.|Glacial conglomerates, diamictites, sandstone, siltstone and shale.|
11718|Merrimelia Formation|67561|6|Mentioned|p67|||||||||
11718|Merrimelia Formation|68068|5|Briefly described|Map legend|Early Permian|Late Carboniferous|Cooper Basin (subsurface only). Age from sparse spore-pollen assemblage. Fluvioglacial outwash, lacustrine (shallow to relatively deep water), subaerial and subaqueous tillites.||Basal unit in Gidgealpa Group.||Is conformably overlain by Tirrawarra Formation.|Buff-white, fine-grained sandstone, rippled, soft-sediment deformation; massive to crudely-bedded conglomerate; poorly-sorted diamictite, matrix-supported, dropstones; dark grey claystone and siltstone, flat-laminated or with sandstone interbeds.|
11718|Merrimelia Formation|68731|5|Briefly described|p200 Fig 3.110, p204, p205, p206|Cisuralian||Cooper Basin. Gravestock et al. (1995) included this formation in the Gidgealpa Group. ~ 80 m thick. A Cisuralian age is suggested based on a basement granite (298 +/- 4 Ma) in the Nappamerri Trough and assignment of palynofloras.||Of the Gidgealpa Group.||Interdigitated with the overlying Tirrawarra Sandstone. Unconformably overlain by the Patchawarra Formation.|Includes proglacial fluvial outwash deposits, termino-glacial fluvial deposits and varvites to delta front debris flows and deepwater lacustrine deposits.|17-JUL-14
11718|Merrimelia Formation|69023|4|Described|p79-83, p163, p191-192|Permian|Late Carboniferous|Cooper Basin. Defined by Martin (1967). Was excluded from the original Gidgealpa Group (Martin, 1967; Gatehouse, 1972) but later included (Callen et al.,1994; Gravestock et al., 1995, and this study). Oil and gas reserves. Fluvio-glacial. Conglomerate clasts mainly from Mooracoochie Volcanics and, locally, reworked glauconite from Pando Formation. Very uneven distribution. 175 to >512m thick. Stratigraphic wells intersection data.||Unit in Gidgealpa Group.||Overlies Dullingari Group. Is overlain by Patchawarra Formation and Tirrawarra Sandstone.|Massive to crudely-bedded conglomerate; fine- to medium-grained sandstone, massive, or flat and planar cross-bedded; subordinate thin, grey-brown siltstone beds and laminations which can be pyritic and carbonaceous; minor shale, coal seams.|
11718|Merrimelia Formation|69454|5|Briefly described|p38:4|Asselian|Asselian|Cooper Basin.||Gidgealpa Group.||Correlated with Crown Point Formation (Pedirka Basin).||12-JUL-16
11718|Merrimelia Formation|69673|6|Mentioned|p153 fig 125|||||Gidgealpa Group||Overlain by Tirrawarra Sandstone||
11718|Merrimelia Formation|69797|5|Briefly described|p17 Fig.2|Late Carbonfierous|Late Carbonfierous|Age: Stephanian (approximated from figure). Geol. Prov: Cooper Basin.||Gidgealpa Group||||
11718|Merrimelia Formation|69946|5|Briefly described|p3, p9, p36, p45, p54|Asselian|Late Carboniferous|Southern Cooper Basin. Glaciofluvial unit deposited unconformably on deformed Warburton Basin strata and exposed granites.||Basal unit in Gidgealpa Group.||Is overlain by Tirrawarra Sandstone conformably and Patchawarra Formation unconformably. Equivalent to Boorthanna Formation (Arckaringa Basin).||
11718|Merrimelia Formation|69947|5|Briefly described|p13 Fig.7.2, p16-17 Figs.7.5-6|Permian|Late Carboniferous|See also p21 Fig.7.10. Cooper Basin.||Gidgealpa Group.||||
11718|Merrimelia Formation|69982|5|Briefly described|p13, p24, p44, Appendix 1|||Cooper Basin. Moolalla 1 gas field, discovered in this unit (Baily, 1990), was later assigned to the Pando Formation in the underlying Warburton Basin. Brief thin section descriptions.||Unit in the Gidgealpa Group.|||Quartz is coarse-grained; muscovite is not altered to chlorite.|
11718|Merrimelia Formation|70317|6|Mentioned|p33|Late Carboniferous|Late Carboniferous|Cooper Basin.||Gidgealpa Group.||Is overlain, locally unconformably, by Tirrawarra Sandstone.||
11718|Merrimelia Formation|70823|4|Described|iv, p25-p27, 51-53|Asselian|Gzhelian|Cooper Basin. Up to 620m thick. Deposited in a terminoglacial, proglacial, glaciolacustrine or aeolian environment. Age debated.Overlies granodiorites with minimum emplacment age of 307 Ma.Palynofloras consistent with APP1.21, 1.22 ie up to top Asselian. Hosts a commercial reservoir that is briefly discussed. See also p36, p40-p41, p51-p53, p78-p80, p82.||Gidgealpa Group||Overlain by and interfingers with the Tirrawarra Sandstone. Underlain by Big Lake Suite granodiorites.|Conglomerate, diamictite, sandstone, conglomeratic mudstone, siltstone and shale.|22-AUG-18
11718|Merrimelia Formation|70824|4|Described|p7-p9, p38-p44, p122|Asselian|Gzhelian|Cooper Basin. Up to 620m thick. Deposited in terminoglacial, proglacial, glaciolacustrine or aeolian environments. Outcrop and areal extent briefly discussed.||||Overlain by the Tirrawarra Sandstone.|Conglomerate, diamictite, sandstone, conglomeratic mudstone, siltstone and shale.|
11718|Merrimelia Formation|70946|5|Briefly described|p1089|Carboniferous|Carboniferous|Cooper Basin. Deposited in a terminoglacial, proglacial, glaciolacustrine and aeolian environments.||Gidgealpa Group.||||08-OCT-18
11718|Merrimelia Formation|71265|5|Briefly described|p589|Asselian|Gzhelian|Cooper Basin.||Gidgealpa Group.||Is overlain by Tirrawarra Sandstone.||
11718|Merrimelia Formation|71342|5|Briefly described|Ch5 p3, Ch5 p9, Ch5 p36, Ch5 p45|Asselian|Stephanian|Cooper Basin. Deposited in a glaciofluvial, proglacial, aeolian or glaciolacustrine envrionment. Palynological zone is given in fig 5.3 Ch5 p36. Thermal history briefly discussed in Ch9. See also Ch5 p54, Ch7 p13, Ch9 p5, Ch9 p10-p11, Ch10 tbl 10.1, Ch10 p14, Ch10 p19-p20.||Gidgealpa Group||Overlain by the Tirrawarra Sandstone.||
11718|Merrimelia Formation|71701|5|Briefly described|p155|Asselian|Kasimovian|Cooper Basin.||Gidgealpa Group||Overlain by the Tirrawarra Sandstone.||
11718|Merrimelia Formation|72478|6|Mentioned|Fig. 7 p70|||||||||
11718|Merrimelia Formation|72497|5|Briefly described|p17 Fig.11, p13.|Early Permian|Late Carboniferous|Cooper Basin. Described as glaciolacustrine, glaciofluvial, tillites environment.||||Underlies Tirrawarra Sandstone with diachronous contact?||
11718|Merrimelia Formation|73167|5|Briefly described|p662, p664, p672|late Carboniferous|late Carboniferous|Cooper Basin. Deposited on regional unconformity above the Warburton Basin. Onlaps onto the Gidgealpa-Merrimelia-Innamincka and Murteree-Nappacoongee ridges. Shown as lower Permian in Fig. 2, p664 and spelt Merrimellia Formation. Contains oil and gas.|||||Glacial sediments.|
11718|Merrimelia Formation|73251|6|Mentioned|p62|Late Carboniferous|Late Carboniferous|Cooper Basin. Terminoglacial, proglacial, glaciolacustrine, and aeolian depositional environments. Contains[?] gas.||Gidgealpa Group||Overlain by Tirrawarra Sandstone.||
11718|Merrimelia Formation|73343|6|Mentioned|p338|Late Carboniferous|Late Carboniferous||||||Glacial sediments.|
11718|Merrimelia Formation|73479|5|Briefly described|p157, p166, p176|Permian|Permian|Base of the Cooper Basin. Glacial unit.|ca 290 Ma|||Underlies Tirrawarra Formation||
11718|Merrimelia Formation|73495|5|Briefly described|p499, p503-504|||Cooper Basin. Deposited in a complex array of glaciolacustrine, terminoglacial and proglacial environments.||Gidgealpa Group||Overlain by and interfingering with Tirrawarra Sandstone. Unconformably overlain by Patchawarra Formation.|Diamictites, sandstones, conglomeratic mudstones, siltstones and shales.|
11790|Middle Camp Granite|22629|6|Mentioned|p157|Proterozoic|Proterozoic|||||||
11790|Middle Camp Granite|22849|5|Briefly described|20|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
11790|Middle Camp Granite|23719|4|Described|p19|Statherian|Statherian|Age: 1757+/-23 Ma (U-Pb zircon). See also page 15 Table 2, page 19 Table 5. Of Lincoln Complex. Geological Province: Gawler Craton.||||||
11790|Middle Camp Granite|23791|6|Mentioned|p5 Fig. 4|||||||||
11790|Middle Camp Granite|24197|5|Briefly described|p74 Tb. 8.1|Paleoproterozoic|Paleoproterozoic|Age: 1750-1700Ma.||||||07-FEB-11
11790|Middle Camp Granite|24526|6|Mentioned|p99|Paleoproterozoic|Paleoproterozoic|Age: 1731+/-7Ma.  Part of the Kimban Orogeny.||||||07-NOV-08
11790|Middle Camp Granite|37461|6|Mentioned|p322|||Variation of Middlecamp ?||||||
11790|Middle Camp Granite|37811|6|Mentioned|Fig.3|||||||||
11790|Middle Camp Granite|39345|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
11790|Middle Camp Granite|39349|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
11790|Middle Camp Granite|39353|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
11790|Middle Camp Granite|39802|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
11790|Middle Camp Granite|40448|5|Briefly described|p34|||||||||
11790|Middle Camp Granite|40644|5|Briefly described|p124 Fig. 3,  p132|Paleoproterozoic|Paleoproterozoic|Included in the Lincoln Complex grouping. Intruded by Carpa Granite. Age: 1650+/-35Ma (p133 Fig. 16).||||||07-NOV-08
11790|Middle Camp Granite|41667|5|Briefly described|p12|||||||||
11790|Middle Camp Granite|41972|6|Mentioned|p367|||||||||
11790|Middle Camp Granite|42738|6|Mentioned|map legend|Mesoproterozoic||||||||
11790|Middle Camp Granite|43052|4|Described|p81,Table 4.4|||Of Lincoln Complex.||||||05-MAR-08
11790|Middle Camp Granite|50605|5|Briefly described|p(i), 1.3, 5.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Gawler Craton and Curnamona Province. Age: 1738 +/- 68Ma (U-Pb). Of the Younger Lincoln Supersuite.||||||07-NOV-08
11790|Middle Camp Granite|60534|5|Briefly described|p573 Fig.2|Paleoproterozoic|Paleoproterozoic|Age: 1700-1750 Ma. Geological Province: Gawler Craton.||||||07-NOV-08
11790|Middle Camp Granite|61262|5|Briefly described|p455 Fig. 11|Paleoproterozoic|Paleoproterozoic|Age: ~1750-1650Ma. Geological Province: western Gawler Craton.||||||07-NOV-08
11790|Middle Camp Granite|61307|5|Briefly described|p39 Fig. 19, p44|Paleoproterozoic|Paleoproterozoic|Age: 1731+/-7Ma. Geological Province: Gawler Craton. See also p48.||||||07-NOV-08
11790|Middle Camp Granite|62893|6|Mentioned|Map Legend, p13-14|Early Proterozoic|Early Proterozoic|Of Parker (1978, 1983). U-Pb zircon age of 1738 +/- 68 Ma (Fanning, 1987).||||||
11790|Middle Camp Granite|63020|5|Briefly described|p987 Fig. 8|Paleoproterozoic|Paleoproterozoic|See also Middlecamp Granite. Age: 1731+/-7Ma. Geological Province: Gawler Craton (Cleve Domain).||||||07-NOV-08
11790|Middle Camp Granite|64130|5|Briefly described|p1381-1382|Statherian|Statherian|Southern Gawler Craton. Syn-Kimban Orogeny. Consists of I-type intermediate and S-type felsic rocks.|1726 +/- 7 Ma (Fanning et al., 2007).|||Intrudes Hutchison Group and Sleaford Complex.||
11790|Middle Camp Granite|64131|6|Mentioned|p1409|||Associated with Kimban orogeny.||||||
11790|Middle Camp Granite|64137|5|Briefly described|p1542 Fig.1, p1544, |Paleoproterozoic|Paleoproterozoic|~1730 Ma (Ferris et al., 2002)||||||
11790|Middle Camp Granite|64313|5|Briefly described|p450 Fig. 1|Paleoproterozoic|Paleoproterozoic|Age: 1737+/-7Ma (U-Pb zircon). Geological province: Gawler Craton.||||||09-FEB-10
11790|Middle Camp Granite|64725|6|Mentioned|p58 Fig.2. |||Gawler Craton.||||||
11790|Middle Camp Granite|65376|5|Briefly described|p9 Fig.1.2, p38, pp74-79. |Paleoproterozoic|Paleoproterozoic|A key unit for constraining timing of Kimban Orogeny, but geochronology ages are inconclusive.|1737 +/- 7 Ma to 1726 +/- 7 Ma.||||Grey, foliated, biotite granite to granodiorite.|
11790|Middle Camp Granite|65390|6|Mentioned|p20, p23 Fig.3|Statherian|Statherian|Cleve Domain, Gawler Craton. Syntectonic with Kimban Orogeny. Intruded at c. 1730 Ma (Fanning, 1997).||||||
11790|Middle Camp Granite|65922|5|Briefly described|p31|Statherian|Statherian|Granite within Lincoln Complex on the YARDEA map sheet is interpreted to be an equivalent of this unit. Age of ~1795-1745 Ma given.||||||
11790|Middle Camp Granite|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.|1736 +/- 6 Ma.|||||
11790|Middle Camp Granite|70383|6|Mentioned|p51|Statherian|Statherian|Mentioned as a possible source of zircons aged c.1732 +/- 20 Ma, extracted from the Sprigg Diamictite Member.||||||
11790|Middle Camp Granite|70721|6|Mentioned|p63|||||||||
11790|Middle Camp Granite|71859|5|Briefly described|p1, p3, p14, p18|||Southern Gawler Craton. Appears as Middlecamp Granite on p1, p3.|1735 Ma|||Intrudes the Minbrie Gneiss.||05-APR-23
11790|Middle Camp Granite|71862|2|Defined|p2, p7, p11-p12, p22|Statherian|Statherian|Named after Middle Camp Homestead, Cleve Hills, central Eyre Peninsula (666465mE, 6272807mN, GDA94, Zone 53). The name was first used by Rutland et al (1981) but never formally defined. The type locality are a series of granite outcrops along the track west-northwest of Ullabidinie Reservoir, Middle Camp Station.  Outcrops extensively in the Cleve Hills on the Eyre Peninsula as broad hill slope exposures and tors. Originally a part of the now obsolete Lincoln Complex. This pluton has an extent of 3.5km east-west and 11km north-south aligned north-northeast with the Kimban structural grain. SHRIMP ages are interpreted as the age of magmatic crystallisation; an additional age of 1726 +/- 7 Ma is derived from Fanning et al, 2007. See also p33-p34, p42, p58-p60.|1736 +/- 6 Ma (Fraser and Neumann, 2010)|Pinbong Suite||Intrudes the Warrow Quartzite and the Minbrie Gneiss.|Grey, moderately to strongly foliated, fine- to medium-grained, equigranular plagiolcase-quartz-K-feldspar-biotite granite.|18-APR-23
11790|Middle Camp Granite|72461|6|Mentioned|p6|||Gawler Craton. Kimban Orogeny.|c. 1730 Ma|||||
11790|Middle Camp Granite|73030|6|Mentioned|p2149|Statherian|Statherian|Gawler Craton.||||||
11790|Middle Camp Granite|73103|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic||||||Grey, foliated, massive, biotite granite and granodiorite with pegmatite veins.|
11790|Middle Camp Granite|73493|6|Mentioned|p716 Fig.3|||Gawler Craton.|||||Granitic.|
11790|Middle Camp Granite|73525|5|Briefly described|p19 Fig.13|Statherian|Statherian|Cleve Domain. See also Middlecamp Granite.|1736+/-6 Ma, 1726+/-7 Ma||||Felsic intrusive.|
11813|Middleback Group|23818|5|Briefly described|p26|||Underlying unit: Warrow Quartzite. Geological Province: Gawler Block.||||||
11813|Middleback Group|30237|6|Mentioned|Fig.1|||||||||
11813|Middleback Group|30806|5|Briefly described|p946|||||||||
11813|Middleback Group|30845|6|Mentioned|p31|||||||||
11813|Middleback Group|31203|6|Mentioned|Fig. 1|||||||||
11813|Middleback Group|31923|6|Mentioned|p5|||||||||
11813|Middleback Group|33470|6|Mentioned|Table 1|||||||||
11813|Middleback Group|33479|6|Mentioned|Fig.1|||||||||
11813|Middleback Group|33557|6|Mentioned|Fig.2|||Geol. map of Gawler Range Volcanic Complex||||||
11813|Middleback Group|33727|6|Mentioned|p36|||||||||
11813|Middleback Group|34116|6|Mentioned|p7|||Precambrian||||||
11813|Middleback Group|34287|6|Mentioned|p33|||||||||
11813|Middleback Group|34319|6|Mentioned|p69|||||||||
11813|Middleback Group|34537|5|Briefly described|p28|||||||||
11813|Middleback Group|34904|6|Mentioned|p141|||||||||
11813|Middleback Group|35078|6|Mentioned|p257|||||||||
11813|Middleback Group|35255|6|Mentioned|p7|||||||||
11813|Middleback Group|35298|5|Briefly described|p946|||||||||
11813|Middleback Group|35495|6|Mentioned|p340|||||||||
11813|Middleback Group|36003|5|Briefly described|p1027|||See also P1031.||||||
11813|Middleback Group|36073|4|Described|p330|||||||||
11813|Middleback Group|36627|6|Mentioned|p81|||||||||
11813|Middleback Group|38068|5|Briefly described|p66|||||||||
11813|Middleback Group|40003|5|Briefly described|Table 3|||||||||
11813|Middleback Group|42190|5|Briefly described|p267|||||||||
11813|Middleback Group|43052|6|Mentioned|p51|||refers to Miles (1954)||||||
11813|Middleback Group|44660|14|Not recorded|map legend||Paleoproterozoic|L.Proterozoic, lithology.||||||07-NOV-08
11813|Middleback Group|61556|5|Briefly described|p8, p9-10 Figure|||Metamorphosed - grey chert, magnetite and ferruginous silicates. Overlie the informally named "Gneiss Complex".||||||21-NOV-07
11813|Middleback Group|66882|5|Briefly described|p99, p103 Fig.3c, p104 Fig.4, p112-118|Neoarchean|Neoarchean|New unit. East of the Kalinjala Mylonite Zone. Provenance solely Archean; deposition occurred in the Archean, or later but with solely Archean detritus. Authors give reasons for the former. Suggested correlation with BIF in the Hamersley Group suggests links between Pilbara and Gawler Cratons.|||Includes Upper Middleback Jaspilite, Cook Gap Schist, Lower Middleback Jaspilite and Katunga Dolomite.||BIF-endowed.|03-MAR-15
11813|Middleback Group|67721|5|Briefly described|p32, p33, p35, p36, p37, p38|Orosirian|Siderian||c. 2500-1730 Ma (Szpunar et al. 2011)|Previously of the Hutchison Group?|Includes Middleback Jaspilite, Upper; Cook Gap Schist, Middleback Jaspilite, Lower; and Katunga Dolomite.|||27-FEB-15
11813|Middleback Group|68208|6|Mentioned|p32 Fig.3, p33, p34 Fig.5|Paleoproterozoic|Paleoproterozoic|Some uncertainty regarding depositional age, which could be as old as Neoarchean, based on work of Szpunar et al. 2011.|||Includes Cook Gap Schist|||
11813|Middleback Group|72058|5|Briefly described|p171-p172, p190|||Middleback Ranges, Gawler Craton. Isotopically and geochemically distinct from the other sedimentary units of the Hutchison Group.|>2565 Ma||Includes the Warrow Quartzite, Katunga Dolomite, Lower and Upper Middleback Iron Formations and the Cook Gap Schist.|Overlies the Sleaford Complex.|Quartzite, dolomite, iron formations and schist.|
11813|Middleback Group|73234|6|Mentioned|p18|Siderian|Archean|Eyre Peninsula, eastern.|Older than c. 2450 Ma||||Metasedimentary rocks.|
11813|Middleback Group|73235|6|Mentioned|p53, p58|Siderian|Neoarchean|Gawler Craton. Spencer, Cleve and Coulta regions. May host gold mineralisation in the Middleback mineral field of the Kimban gold mineral system but no gold-only discoveries are yet known.|c. 2530-2410 Ma|||||
11826|Middleton Sandstone|22581|5|Briefly described|Fig.2,p37|||Kanmantoo Group, Kanmantoo Basin. Overlies Petrel Cove Formation||||||
11826|Middleton Sandstone|22643|5|Briefly described|fig3,6,7|Cambrian|Cambrian|||||||
11826|Middleton Sandstone|22840|6|Mentioned|Table1 P38|||||||||
11826|Middleton Sandstone|23539|5|Briefly described|Fig 1 p 467|||||||||
11826|Middleton Sandstone|23981|5|Briefly described|p13|Early Cambrian|Early Cambrian|Of the Kanmantoo Group. Geological Province: Stansbury Basin (Fleurieu Peninsula).||||||04-FEB-08
11826|Middleton Sandstone|24465|4|Described|p357|Early Cambrian|Early Cambrian|Of the Bollaparudda Subgroup. Possibly a structural repeat of the Backstairs Passage Formation. See also Middleton Formation. See also p346 Fig. 3.||||||27-MAY-08
11826|Middleton Sandstone|30380|6|Mentioned|Table 1|||Correlation||||||
11826|Middleton Sandstone|30381|3|Fully described|p221|||See also p222.||||||26-JUN-08
11826|Middleton Sandstone|32457|6|Mentioned|p90|||||||||
11826|Middleton Sandstone|35255|6|Mentioned|Fig.8|||||||||
11826|Middleton Sandstone|36836|6|Mentioned|Table 1|||||||||
11826|Middleton Sandstone|38699|6|Mentioned|p19|||||||||
11826|Middleton Sandstone|38873|4|Described|Table 2|||||||||
11826|Middleton Sandstone|40442|6|Mentioned|p17|||||||||
11826|Middleton Sandstone|40454|5|Briefly described|p46|||||||||
11826|Middleton Sandstone|40455|5|Briefly described|p71|||||||||
11826|Middleton Sandstone|40856|6|Mentioned|Fig.23.6|||||||||
11826|Middleton Sandstone|41947|6|Mentioned|Fig.2 P17|||||||||
11826|Middleton Sandstone|42222|5|Briefly described|p21|||||||||
11826|Middleton Sandstone|42225|6|Mentioned|Fig.4 P224|||||||||
11826|Middleton Sandstone|42270|6|Mentioned|p353|||||||||
11826|Middleton Sandstone|42271|6|Mentioned|p372|||||||||
11826|Middleton Sandstone|42272|5|Briefly described|p404|||||||||
11826|Middleton Sandstone|42273|6|Mentioned|Fig.19 P437|||(Kanmantoo Group)||||||
11826|Middleton Sandstone|43052|5|Briefly described|Table 2.1|||||||||
11826|Middleton Sandstone|43703|6|Mentioned|Fig.1,p75|||||||||
11826|Middleton Sandstone|43759|6|Mentioned|p445|||||||||
11826|Middleton Sandstone|44133|5|Briefly described|p4 Fig. 7.2, 17, 18|Middle Cambrian|Middle Cambrian|Geological Province: Stansbury Basin. Of ther Kanmantoo Group. Overlies: Petrel Cove Formation.||||||
11826|Middleton Sandstone|60712|5|Briefly described|p28 Fig. 1, p30 Fig. 3|Early Cambrian|Early Cambrian|Of the Wattaberri Subgroup (Kanmantoo Group). Of Daily and Milnes (1972, 1973).||||||27-MAY-08
11826|Middleton Sandstone|61307|5|Briefly described|p6 Fig. 3, p7|Cambrian|Cambrian|Of the Kanmantoo Group. Inturded by the Victor Harbor Granite. Geological Province: Adelaide Fold Belt.||||||15-JAN-08
11826|Middleton Sandstone|64282|5|Briefly described|Map legend|Early Cambrian|Early Cambrian|Of the Kanmantoo Group. Geological Province: Kanmantoo Trough. Medium-grained grey sandstone; laminated x-bedded with slump bedding. Large scale tabular crossbeds up to 1-3m with heavy mineral lamination in toesets and slumped tops to foresets.||||||24-JUL-08
11826|Middleton Sandstone|65375|5|Briefly described|p33.|Middle Cambrian|Middle Cambrian|||Unit in Kanmantoo Group.||Overlies Petrel Cove Formation.||
11826|Middleton Sandstone|65664|5|Briefly described|p1096, p1101-5, Tabs.1-4, p1106 Fig.5|Early Cambrian|Early Cambrian|Shallow water depositional environment. In tectonic contact with other Kanmantoo Group units. Lithologically similar to Backstairs Passage Formation, and may be an equivalent.||Of Bollaparudda Subgroup.||||09-MAY-12
11826|Middleton Sandstone|65892|5|Briefly described|p9 Fig.4. |Middle Cambrian|Middle Cambrian|Fleurieu Peninsula.||Unit in Kanmantoo Group.||Overlies Petrel Cove Formation.||
11826|Middleton Sandstone|65921|5|Briefly described|p1, p2 (map legend).|Cambrian|Cambrian|Occurs at Cape Gantheaume, Seal Bay and Cape du Couedic. This Formation is cross-cut by igneous dykes. Rhythmic cyclicity in sedimentary structures is indicative of sandwave sedimentation in a tidal-dominated shallow sea.||Of the Kanmantoo Group.|||Shallow marine sandstones with heavy mineral bands.|10-JAN-17
11826|Middleton Sandstone|68735|5|Briefly described|p235 Fig.3|Middle Cambrian|Middle Cambrian|Fleurieu Peninsula.||Of the Kanmantoo Group.||||10-APR-17
11826|Middleton Sandstone|68993|6|Mentioned|p544 Fig.1|Middle Cambrian|Middle Cambrian|Fleurieu Peninsula.||Of the Kanmantoo Group.||||
11826|Middleton Sandstone|73107|5|Briefly described|Map legend.|Early Cambrian|Early Cambrian|Kanmantoo Trough.||Kanmantoo Group.|||Medium-grained grey metasandstone. Laminated, cross-bedded and slumped bedding. Large scale tabular crossbeds up to 1 to 3 metres with heavy mineral laminations in toesets and slumped tops to foresets.|
11826|Middleton Sandstone|73188|6|Mentioned|p316|Early Cambrian|Early Cambrian|Mount Lofty Ranges.||Bollaparudda Subgroup, Kanmantoo Group|||Cross-bedded feldspathic sandstone.|
11846|Millers Creek Dolomite Member|24175|5|Briefly described|p40|Tertiary|Tertiary|Of the Mirikata Formation.  White silicified dolomite and and limestone with minor sepiolite.  Overlies Danae Conglomerate Member.  Geological Province: Billa Kalina Basin.||||||
11846|Millers Creek Dolomite Member|24321|5|Briefly described|Map legend|Miocene|Miocene|Parent: Mirikata Formation||||||
11846|Millers Creek Dolomite Member|31532|6|Mentioned|Table 1|||||||||
11846|Millers Creek Dolomite Member|36213|6|Mentioned|p85|||||||||
11846|Millers Creek Dolomite Member|36966|4|Described|p85|||||||||
11846|Millers Creek Dolomite Member|38604|6|Mentioned|Map legend|Miocene|Miocene|||||||
11846|Millers Creek Dolomite Member|38605|6|Mentioned|p30|||See also Table 5.||||||
11846|Millers Creek Dolomite Member|42375|6|Mentioned|p79, p86|||Mbr of Mirikata Formation||||||
11846|Millers Creek Dolomite Member|42465|5|Briefly described|Map Legend|||||||||
11846|Millers Creek Dolomite Member|42469|4|Described|p39|||Billa Kalina Basin||||||
11846|Millers Creek Dolomite Member|42723|5|Briefly described|map legend|Miocene||||||||
11846|Millers Creek Dolomite Member|43048|4|Described|Table 3.|||||||||
11846|Millers Creek Dolomite Member|43052|5|Briefly described|Table 2.1|||of Mirikata Formation||||||
11846|Millers Creek Dolomite Member|44133|4|Described|p190 Fig. 10.30|Miocene|Miocene|Geological Province: Billa Kalina Basin. Of the Mirikata Formation. Thickness: 10m. Overlies Billa Kalina Clay Member gradationally.||||||
11846|Millers Creek Dolomite Member|64696|5|Briefly described|p133 Figs.13,14 |Miocene|Miocene|||Of the Mirikata Formation.||||
11846|Millers Creek Dolomite Member|66520|5|Briefly described|p11-12. |Tertiary|Tertiary|6 m thick.||Unit in Mirikata Formation.|||Cream to white dolomite, dolomitic limestone.|
11846|Millers Creek Dolomite Member|67462|5|Briefly described|Map legend.|Miocene|Miocene|Billa Kalina Basin.||Unit in Mirikata Formation.||||
11846|Millers Creek Dolomite Member|68715|6|Mentioned|p30 Fig.5|Miocene|Miocene|Billa Kalina Basin. Middle to Late Miocene age.||||||
11872|Millyera Formation|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.||||Overlies the Yandruwantha Sand.||
11872|Millyera Formation|22912|5|Briefly described|33|||||||||
11872|Millyera Formation|23154|5|Briefly described|Map Legend|Late Pleistocene|Late Pleistocene|Geological Province - Lake Eyre Basin - Callabonna Basin.||||||
11872|Millyera Formation|23155|5|Briefly described|p37|Late Pleistocene|Late Pleistocene|A massive gypsum crust commonly caps these lake deposits.||||||
11872|Millyera Formation|30055|4|Described|p156|||Mention p153.||||||07-SEP-18
11872|Millyera Formation|30056|2|Defined|p142|Pleistocene|Pleistocene|||||||
11872|Millyera Formation|36620|5|Briefly described|Fig.1|||See also p24.||||||07-SEP-18
11872|Millyera Formation|38682|6|Mentioned|Fig.3|||||||||
11872|Millyera Formation|39085|6|Mentioned|p13|||||||||
11872|Millyera Formation|39804|1|Redefined|p165|Quaternary|Quaternary|||||||
11872|Millyera Formation|39902|6|Mentioned|Fig.5|||||||||
11872|Millyera Formation|40756|6|Mentioned|Fig.1.2|||||||||
11872|Millyera Formation|40914|6|Mentioned|Map legend|Cenozoic|Cenozoic|||||||19-NOV-08
11872|Millyera Formation|41125|6|Mentioned|Table 10|||||||||
11872|Millyera Formation|41537|6|Mentioned|Fig.2|||||||||
11872|Millyera Formation|42090|3|Fully described|p38|||||||||
11872|Millyera Formation|42592|6|Mentioned|p280|||Lake Frome.||||||07-SEP-18
11872|Millyera Formation|42746|5|Briefly described|p22|||||||||
11872|Millyera Formation|44133|5|Briefly described|p247, 244 Table 11.3|Late Pleistocene|Middle Pleistocene|Maximum Thickness: 9m.||||||
11872|Millyera Formation|46815|6|Mentioned|p250|||Refers to type sections.||||||
11872|Millyera Formation|60953|5|Briefly described|Map Legend|Pleistocene|Pleistocene|Fossiliferous clay, sandy clay, minor limestone.||||||
11872|Millyera Formation|61108|5|Briefly described|map legend|Pleistocene|Pleistocene|Lacustrine sediments of playas and lakes: fossiliferous clay, sandy clay and minor limestone.||||||
11872|Millyera Formation|61155|5|Briefly described|p17|Pleistocene|Late Pliocene|Overlain by Eurinilla Formation. Age: 2.5-1.5Ma.  Geological Province: Tarkarooloo Basin.||||||
11872|Millyera Formation|65925|5|Briefly described|pp17-18.|Pleistocene|Pleistocene|Flood-plain and lacustrine deposits of Lake Frome. Up to 9m thick.||||Intertongues with Coomb Spring Formation.|Greenish clay, thin algal limestone, fine-grained white to greenish sand.|
11872|Millyera Formation|66131|6|Mentioned|p246-247|Pleistocene|Pleistocene|Lake Callabonna area. Contains the famous Late Pleistocene vertebrate fauna.||||Intertongues with Coomb Spring Formation.||
11872|Millyera Formation|66518|6|Mentioned|p19 Fig.4.|Cenozoic|Cenozoic|Lake Eyre Basin.||||Overlies Namba Formation and is overlain by Coonarbine Formation and equivalents. Is shown as age-equivalent to Willawortina and Eurinilla Formations.||
11872|Millyera Formation|68068|5|Briefly described|Map legend|Pleistocene|Pleistocene|Callabonna Sub-basin, Lake Eyre Basin. In part equivalent to Coomb Spring Formation. Contains the Lake Callabonna megafauna in its upper part; also fish bones, mollusc shells, ostracods, wood and algal remains. Part-equivalent to Coomb Spring Formation.||||Overlies, locally intertongues with, Willawortina Formation. Interdigitates with Eurinilla Formation. Is overlain by Coomb Spring Formation.|Green to grey clay with subconchoidal fracture or soft and crumbly, interbedded fine sand and silt, persistent limestone lamellae near top.|
11872|Millyera Formation|69019|4|Described|p106 Fig.26, p120-121, p166-167.|Pleistocene|Pleistocene|W of Lake Blanche. Originally Millyera Beds (Callen and Tedford, 1976); revised to Formation status by Callen (1990). Hosts the Lake Callabonna megafauna fossil horizon; fossil fauna listed. Age-dating discussed. Hosts celestite layers, nodules and concretions.|128,000 to 10,000 y BP (Callen, 1984).|||Disconformably overlies Namba Formation.|Unconsolidated; green clay with alternating silt and very fine sand beds, with persistent limestone laminations near the top grading laterally into rippled gypsum; commonly crusted by ~1 m thick gypsum.|
11872|Millyera Formation|69023|5|Briefly described|p109, p126-127, p133, p142, p161|Pleistocene|Pleistocene|Originally Millyera Beds of Callen and Tedford (1976); elevated to Formation status by Callen (1990). Represents lacustrine facies of paleo-lakes in alternating dry and wet intervals in Quaternary SA. Originally defined in Lake Frome area; subsequently extended N and NW. Hosts stratiform layers, nodules and concretions of celestite.||||Intertongues with Willawortina Formation; disconformably overlies Namba Formation and (locally) Willawortina Formation.|Unconsolidated: green clay with alternating silt and very fine sand beds; persistent limestone laminations near the top grading laterally into rippled gypsum; fine cross-bedding to wavy horizontal bedding is typical; massive ~1m thick gypsum crust.|
11872|Millyera Formation|69648|6|Mentioned|p29|||Lake Eyre Basin. Mis-spelt as Milyera.||||Similar to Ilkina Formation (Eucla Basin).||
11872|Millyera Formation|69947|5|Briefly described|p13 Fig.7.2|Pleistocene|Pleistocene|Callabonna Sub-basin, Lake Eyre Basin.||||||
11872|Millyera Formation|71342|6|Mentioned|Ch7 p13|Middle Pleistocene|Early Pleistocene|||||Overlies the Yandruwantha Sand.||
11872|Millyera Formation|72456|5|Briefly described|Map Legend|Pleistocene|Pleistocene|Marree 1:250k map sheet.  Age is 145 000 to 60 000-30 000 years BP. Deposited in a lacustrine to floodplain environment.|||||Clay, greenish, thin algal limestone; fine-grained, white to greenish sand.|
11872|Millyera Formation|73251|6|Mentioned|p36, p62|Cenozoic|Cenozoic|Lake Eyre Basin, Callabonna Sub-basin / Poontana Trough. Thermally sub-mature. Lacustrine and floodplain depositional environments.||||Underlain by Namba Formation. Overlain by Coonarbine Formation. Equivalent to Eurinilla Formation and Willawortina Formation.||
11923|Minmi Member|23982|5|Briefly described|p58 Fig.18|||Of Bungil Formation. Geological Province: Surat Basin.||||||
11923|Minmi Member|24092|5|Briefly described|p8 Fig.3|||Of Bungil Formation. Geological Province: Surat Basin.||||||
11923|Minmi Member|30020|6|Mentioned|p30|||||||||
11923|Minmi Member|30021|6|Mentioned|p87|||||||||
11923|Minmi Member|30022|6|Mentioned|p28|||||||||
11923|Minmi Member|30024|6|Mentioned|p336|||||||||
11923|Minmi Member|30446|6|Mentioned|p39|||||||||
11923|Minmi Member|30691|5|Briefly described|p21|||Of Blythesdale Formation||||||
11923|Minmi Member|30694|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
11923|Minmi Member|30695|4|Described|Table 4|||Lower Cretaceous age||||||
11923|Minmi Member|30696|4|Described|Table 4|||Lower Cretaceous age||||||
11923|Minmi Member|30702|6|Mentioned|p21|||Of Blythesdale Formation||||||
11923|Minmi Member|30771|6|Mentioned|p4|||Cretaceous.Member of Hackdown Formation||||||
11923|Minmi Member|31116|4|Described|p41|||See also p42.||||||08-MAR-19
11923|Minmi Member|31208|6|Mentioned|Table 1|||||||||
11923|Minmi Member|32193|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
11923|Minmi Member|32314|6|Mentioned|Fig. 4|||||||||
11923|Minmi Member|32796|6|Mentioned|p302|||||||||
11923|Minmi Member|34543|6|Mentioned|p98|||||||||
11923|Minmi Member|34613|6|Mentioned|p15|||||||||
11923|Minmi Member|34619|6|Mentioned|p.160, Pl.22||Adelaidean|||||||
11923|Minmi Member|35855|6|Mentioned|Fig.2|||Early Cretaceous lithostratigraphy.||||||
11923|Minmi Member|36357|5|Briefly described|p77|||||||||
11923|Minmi Member|36552|6|Mentioned|p59|||||||||
11923|Minmi Member|36571|6|Mentioned|Table 4|||||||||
11923|Minmi Member|36574|6|Mentioned|p602|||||||||
11923|Minmi Member|37995|6|Mentioned|p66|||||||||
11923|Minmi Member|38373|6|Mentioned|p621|||||||||
11923|Minmi Member|38374|6|Mentioned|p605|||||||||
11923|Minmi Member|39211|5|Briefly described|p31|||||||||
11923|Minmi Member|39212|4|Described|p40|||Excursion site. See also p18.||||||08-MAR-19
11923|Minmi Member|39216|6|Mentioned|p55|||Fauna||||||
11923|Minmi Member|40541|4|Described|p111|||||||||
11923|Minmi Member|40666|4|Described|p358|||||||||
11923|Minmi Member|41057|6|Mentioned|p61|||||||||
11923|Minmi Member|41064|6|Mentioned|p60|||||||||
11923|Minmi Member|41266|6|Mentioned|Fig.3|||||||||
11923|Minmi Member|41427|6|Mentioned|p84|||||||||
11923|Minmi Member|42494|5|Briefly described|Table 1 P24|||||||||
11923|Minmi Member|43989|14|Not recorded|Map Legend||Early Cretaceous|||||||
11923|Minmi Member|44021|14|Not recorded|p232(Fig.1)|||||||||
11923|Minmi Member|44031|14|Not recorded|p11||Early Cretaceous|||||||
11923|Minmi Member|44082|6|Mentioned|p8,10,Tb.p34|||Part of Blythesdale Group. Mentioned with respect to Qld Cretaceous fossils which are either of stratigraphic significance or are illustrative of the occurrence of a particular group.||||||
11923|Minmi Member|44376|4|Described|p1-9,11-8,20-3,25,29|||Fossils.||||||
11923|Minmi Member|44377|2|Defined|p1,2,10,13,map||Aptian|Top-most member of Blythesdale Formation. marine Aptian, mainly "calcareous and glauconitic protoquartzites", probably "near-shore facies equivalents of sediments in the lower part of the Roma Formation."||||||
11923|Minmi Member|44915|14|Not recorded|p18|||Ref. to Vine and Day 1965.||||||
11923|Minmi Member|45110|3|Fully described|p112|||See also p10. Of Bungil Formation.||||||08-MAR-19
11923|Minmi Member|45132|6|Mentioned|Table 2|||||||||
11923|Minmi Member|46791|6|Mentioned|Table 1|||||||||
11923|Minmi Member|46937|5|Briefly described|Fig.10|||See also Table 1.||||||
11923|Minmi Member|46984|6|Mentioned|Table 1|||||||||
11923|Minmi Member|48919|4|Described|Table 5|||||||||
11923|Minmi Member|48920|6|Mentioned|p59|||See also P73. Member of Blythesdale Formation.||||||
11923|Minmi Member|49010|6|Mentioned|Fig.4|||Surat Basin||||||
11923|Minmi Member|49011|6|Mentioned|Fig.3|||Surat Basin||||||
11923|Minmi Member|64856|4|Described|p98,99|early Aptian|early Aptian|Of Day (1964). Originally included in Blythesdale Formation, now in Bungil Formation. Contains early Aptian dinoflagellate assemblages.|| ||||31-JAN-13
11923|Minmi Member|65384|5|Briefly described|S116, S117, S118|||Probably Aptian.Of Bungil Formation, Surat Basin.||||||
11923|Minmi Member|66529|6|Mentioned|p12 Fig.5 |||Surat Basin.||Unit in Bungil Formation.||Overlies Nullawurt Sandstone Member.||
11923|Minmi Member|66623|6|Mentioned|p449.|Early Cretaceous|Early Cretaceous|Contains various bivalve species which occur also in the Milparinka-Tibooburra district (Rolling Downs Group).||||||
11923|Minmi Member|69594|5|Briefly described|p538|Aptian|Aptian|Northern Surat Basin. Previously included by Day (1964) in his Blythesdale Formation. The type area is near Bungil Creek at Minmi Crossing. Contains a sproradic but diverse marine fauna dominated by molluscs, and the dinosaur Minmi paravertebra. Marine and brackish water environment.||Bungil Formation.|||Calcareous and glauconitic sandstones, silty shales and siltstones and minor intraformational conglomerates.|
11923|Minmi Member|70821|5|Briefly described|p80|||Surat Basin.||Bungil Formation.||Overlies Nullawurt Sandstone Member. Is overlain by Doncaster Member (Wallumbilla Formation).||
11923|Minmi Member|71601|6|Mentioned|p121|Aptian|Aptian|||Bungil Formation||||
11923|Minmi Member|72298|5|Briefly described|p801|Cretaceous|Cretaceous|Surat Basin (QLD,NSW).||Bungil FZ.||Overlies Nullawurt Sandstone Member. Is overlain by Doncaster Member (Wallumbilla FZ).||
11940|Mintabie beds|23288|6|Mentioned|Fig.5||Early Ordovician|||||||
11940|Mintabie beds|23858|5|Briefly described|p917|Ordovician|Cambrian|Geological Province: Officer Basin.||||||
11940|Mintabie beds|42346|5|Briefly described|p81, Fig.4 p82|||Age Ordovician?||||||
11940|Mintabie beds|43052|5|Briefly described|Fig.2.10|||||||||
11940|Mintabie beds|43053|5|Briefly described|Map Legend|Devonian|Ordovician|Fluviodeltaic sandstone and siltstone.||||||25-MAY-05
11940|Mintabie beds|43258|5|Briefly described|Map Legend|Devonian|Ordovician|||||||
11940|Mintabie beds|43298|5|Briefly described|Map Legend|Devonian|Ordovician|||||||
11940|Mintabie beds|44133|5|Briefly described|p40-41, 4 Fig. 7.2|Devonian|Devonian|Geological Province: Eastern Officer Basin. Overlies: Cartu beds and Blue Hills Sandstone..||||||
11940|Mintabie beds|60953|5|Briefly described|Map Legend|Silurian|Silurian|Of the Munda Group.||||||27-APR-05
11940|Mintabie beds|61108|5|Briefly described|map legend|Silurian|Silurian|Of Munda Group. Shallow marine to fluviodeltaic sandstone, siltstone and shale. Age: ?Silurian.||||||02-JUN-05
11940|Mintabie beds|73090|5|Briefly described|p3, p4 Fig.2, p5-6, p11-14, Appendix|Silurian|Ordovician|Hosts one of the most economically important opal fields in Australia.|||||A lower unit of interbedded weathered shales, siltstones and sandstones; an upper unit of variably silicified, kaolinitic, massive to cross-bedded, fine to medium sandstones, and coarser-grained quartzose sandstones with clay interbeds and lenses.|
11942|Mintaro Shale|22889|6|Mentioned|p35 & p37|Adelaidean|Adelaidean|Parent - Belair Subgroup. The former correlation of the Mintaro Shale with the Glen Osmond Slate (Preiss et al., 1993)(now superseded by the Glen Osmond Slate Member this article) is no longer supported.||||||
11942|Mintaro Shale|23731|6|Mentioned|p27|||||||||
11942|Mintaro Shale|23818|5|Briefly described|p62|Adelaidean|Adelaidean|Of the Belair Sub-Group. Max. thickness: 4500 ft.||||||
11942|Mintaro Shale|29780|6|Mentioned|p28|||||||||
11942|Mintaro Shale|30801|6|Mentioned|p5|||Table P5-6||||||
11942|Mintaro Shale|30807|6|Mentioned|p103|||Suggested map symbol||||||
11942|Mintaro Shale|32319|6|Mentioned|p108|||Geological map||||||
11942|Mintaro Shale|32506|6|Mentioned|p116|||||||||
11942|Mintaro Shale|32510|6|Mentioned|p106|||See also Table 1||||||
11942|Mintaro Shale|33474|6|Mentioned|Fig.2|||||||||
11942|Mintaro Shale|33577|6|Mentioned|p80|||Geol. map. Shale deposits P79.||||||
11942|Mintaro Shale|34535|6|Mentioned|p62|||See Fig.19.  Belair Sub-Gp.||||||
11942|Mintaro Shale|34536|6|Mentioned|Map legend|Precambrian|Precambrian|Sturtian||||||
11942|Mintaro Shale|34587|5|Briefly described|p36|||||||||
11942|Mintaro Shale|36126|6|Mentioned|Fig.1|||||||||
11942|Mintaro Shale|36625|6|Mentioned|Fig.1|||||||||
11942|Mintaro Shale|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Torrensian||||||
11942|Mintaro Shale|41404|4|Described|p114|||Mention P107||||||
11942|Mintaro Shale|42098|5|Briefly described|p53|||||||||
11942|Mintaro Shale|42222|5|Briefly described|p15|||||||||
11942|Mintaro Shale|42720|5|Briefly described|map legend|Sturtian|Torrensian|||||||
11942|Mintaro Shale|42813|5|Briefly described|p17|||Of Burra Group||||||25-JAN-08
11942|Mintaro Shale|43052|5|Briefly described|p181,Table 6.1|||Of Burra Group.||||||06-MAY-09
11942|Mintaro Shale|44659|5|Briefly described|map legend|||Sturtian, lithology.||||||
11942|Mintaro Shale|44690|4|Described|map legend|||Geol. Atlas Series. (I/54-5). Sturtian.||||||
11942|Mintaro Shale|61732|5|Briefly described|p28 Fig. 13|Sturtian|Sturtian|Of the Belair Subgroup (Umberatana Group). Includes the Leasingham Quartzite Member. Geological Province: Adelaide Rift Complex.||||||07-FEB-11
11942|Mintaro Shale|62724|5|Briefly described|p16, p17 Fig. 4|Sturtian|Torrensian|Of Belair Subgp (Burra Gp). Lower siltst unit containing some thin interbeds of sandy dolomite and greywacke towards the top; interfingers with clean, med.-gr. sandst and quartzite tongues and through-going into the overlying Gilbert Range Quartzite.||||||07-FEB-11
11942|Mintaro Shale|64769|6|Mentioned|p27|||SA. Mintaro Slate dimension stone is from this unit.||||||06-MAY-09
11942|Mintaro Shale|64796|6|Mentioned|p191 Fig.9|Neoproterozoic|Neoproterozoic|Appears in Fig.9 without the lithology/rank.||Unit in Belair Subgroup.||Overlies Saddleworth Formation.||
11942|Mintaro Shale|70405|5|Briefly described|p50|Cryogenian|Cryogenian|||Belair Subgroup|||Laminated siltstone with an upward increase of fine-medium grained sandy intercalations, vary from clean sandstone to immature greywacke. 100m thickness exposed, 400m total thickness (possibly).|
11942|Mintaro Shale|70819|5|Briefly described|p11, 13, p15 Fig.6, p16, p22-24, 26-28|Neoproterozoic|Neoproterozoic|Clare Valley. Quarried for slate since early 1850s. Represents a marine transgression. Appears also as Mintaro Shale Formation. Forms gently undulating terrain. See also p30.||Belair Subgroup.||Overlies Leasingham Quartzite. Is overlain by Gilbert Range Quartzite.|Flaggy, laminated siltstones.|
11942|Mintaro Shale|71237|14|Not recorded|p9, 18|||||||||
11942|Mintaro Shale|74367|6|Mentioned|p7 Fig.6|||||Belair Subgroup||||
11952|Mirackina Conglomerate|23054|5|Briefly described|p28|Miocene|Eocene|||||||
11952|Mirackina Conglomerate|23719|6|Mentioned|p29|||Geological Province: Gawler Craton.||||||
11952|Mirackina Conglomerate|29658|2|Defined|p2|late Miocene|late Miocene|||||||
11952|Mirackina Conglomerate|29659|6|Mentioned|p9|||||||||
11952|Mirackina Conglomerate|29660|6|Mentioned|p7|||||||||
11952|Mirackina Conglomerate|30924|6|Mentioned|Map legend|Miocene|Miocene|Prob. Miocene||||||
11952|Mirackina Conglomerate|35080|6|Mentioned|p14|||||||||
11952|Mirackina Conglomerate|36966|6|Mentioned|p88|||||||||
11952|Mirackina Conglomerate|39322|6|Mentioned|p404|||||||||
11952|Mirackina Conglomerate|39349|6|Mentioned|Map legend|Miocene|Oligocene|Oligocene to Miocene||||||
11952|Mirackina Conglomerate|40910|6|Mentioned|p18|||||||||
11952|Mirackina Conglomerate|40911|6|Mentioned|Map legend|Miocene|Miocene|Prob. Miocene||||||
11952|Mirackina Conglomerate|42469|5|Briefly described|p39|||||||||
11952|Mirackina Conglomerate|43053|5|Briefly described|Map Legend|Pliocene|Miocene|Silcreted fluvial conglomerate and sand. Geological Province: Lake Eyre Basin.||||||25-MAY-05
11952|Mirackina Conglomerate|43258|5|Briefly described|Map Legend|Pliocene|Miocene|||||||
11952|Mirackina Conglomerate|43298|5|Briefly described|Map Legend|Pliocene|Miocene|||||||
11952|Mirackina Conglomerate|43681|4|Described|p296|||||||||
11952|Mirackina Conglomerate|44133|5|Briefly described|p193, 190 Fig. 10.30|Middle Miocene|Middle Eocene|Geoloigcal Province: Lake Eyre Basin.||||||
11952|Mirackina Conglomerate|44289|5|Briefly described|Map Legend|Pliocene|Eocene|||||||
11952|Mirackina Conglomerate|60953|5|Briefly described|Map Legend|Pliocene|Miocene|Silcreted fluvial conglomerate and sand. Geological Province: Lake Eyre Basin.||||||
11952|Mirackina Conglomerate|61108|5|Briefly described|map legend|Pliocene|Miocene|Silcreted fluvial conglomerate and sand. Geological Province: Lake Eyre Basin.||||||
11952|Mirackina Conglomerate|61155|5|Briefly described|p17|Middle Miocene|Early Miocene|Geological region: Oodnadatta area.||||||
11952|Mirackina Conglomerate|66131|6|Mentioned|p242 Fig.2, p249|Miocene|Eocene|Middle Eocene to Early Miocene in age (from p.242 Fig.2 - stratigraphic correlation chart). Ferricrete in this unit is widespread in the southwestern part of Lake Eyre Basin.||||||
11952|Mirackina Conglomerate|67120|5|Briefly described|Map legend|Miocene|Eocene||||||Conglomerate with silcrete clasts, medium to coarse-grained sandstone, fluvial. Fine-grained sand in siltstone and shale near top.|
11952|Mirackina Conglomerate|67462|5|Briefly described|Map legend.|Neogene|Paleogene|Shown as two seperate units. One Eocene & equivalent to Eyre Formation, the younger one Miocene and in both Tirari Sub-basin, Lake Eyre Basin and Stevenson-Mirackina Region.||||||04-DEC-13
11952|Mirackina Conglomerate|68715|6|Mentioned|p30 Fig.5|Neogene|Eocene|Stevenson-Mirackina Region and Tirari and northern Callabonna sub-basins. Lake Eyre Basin.||||||
11952|Mirackina Conglomerate|69019|5|Briefly described|p105 Fig.25.|Miocene|Eocene|Tirari Sub-basin.||||Is overlain by Etadunna Formation.||
11952|Mirackina Conglomerate|69023|6|Mentioned|p108|Miocene|Miocene|Tirari Sub-basin, Lake Eyre Basin.||||||
11952|Mirackina Conglomerate|69946|5|Briefly described|p29, p129|Oligocene|Oligocene|Uplifted silcretes were reworked to form this unit, which occurs in palaeochannels around the Lake Eyre Basin.||||||
11952|Mirackina Conglomerate|70336|5|Briefly described|Map legend|Miocene|Eocene||||||Conglomerate with silcrete clasts, medium- to coarse-grained sandstone. Fluvial. Fine-grained sand in siltstone and shale near top.|
11952|Mirackina Conglomerate|70938|5|Briefly described|p807-808, p814|Cenozoic|Cenozoic|A palaeochannel deposit.||||||13-DEC-19
11952|Mirackina Conglomerate|71342|6|Mentioned|Ch5 p29, Ch5 p130|Middle Miocene|Early Eocene|Lake Eyre Basin. Occurs in palaeochannels around the Lake Eyre Basin.||||||
11961|Mirikata Formation|24175|5|Briefly described|p40|Tertiary|Tertiary|See also p36, 38.||||||
11961|Mirikata Formation|24321|5|Briefly described|Map legend|Miocene|Miocene|Contains the Millers Creek Dolomite Member.||||||
11961|Mirikata Formation|36966|3|Fully described|p89|||||||||
11961|Mirikata Formation|38022|6|Mentioned|Fig.4|||||||||
11961|Mirikata Formation|38108|6|Mentioned|Table 1|||||||||
11961|Mirikata Formation|40664|6|Mentioned|p246|||||||||
11961|Mirikata Formation|42247|5|Briefly described|Fig.3 P7|||||||||
11961|Mirikata Formation|42375|6|Mentioned|p32, p79|||Billa Kalina Basin||||||
11961|Mirikata Formation|42465|5|Briefly described|Map Legend|||||||||
11961|Mirikata Formation|42469|4|Described|p39|||Billa Kalina Basin||||||
11961|Mirikata Formation|42723|5|Briefly described|map legend|Miocene||||||||
11961|Mirikata Formation|43048|4|Described|Table 3.|||||||||
11961|Mirikata Formation|43052|5|Briefly described|Table 2.1|||||||||
11961|Mirikata Formation|43053|5|Briefly described|Map Legend|Pliocene|Miocene|Geological Province: Billa Kalina Basin||||||25-MAY-05
11961|Mirikata Formation|43258|5|Briefly described|Map Legend|Pliocene|Miocene|||||||
11961|Mirikata Formation|43298|6|Mentioned|Map Legend|Pliocene|Miocene|||||||
11961|Mirikata Formation|44133|4|Described|p197, 190 Fig. 10.30|Miocene|Miocene|Geological Province: Billa Kalina Basin. Thickness: 15m. Includes: Danae Conglomerate Member, Billa Kalina Clay Member, Millers Creek Dolomite Member.||||||
11961|Mirikata Formation|60953|5|Briefly described|Map Legend|Pliocene|Miocene|Geological Province: Billa Kalina Basin.||||||
11961|Mirikata Formation|60955|5|Briefly described|Map Legend|Miocene|Eocene|Includes Watchie Sandstone Member. Sandstones, siltstones and minor clays, partially silicified.||||||
11961|Mirikata Formation|61108|5|Briefly described|map legend|Pliocene|Miocene|Lacustrine dolomite, clay, sand and silt. Geological Province: Billa Kallina Basin.||||||
11961|Mirikata Formation|61155|5|Briefly described|p17|Middle Miocene|Early Miocene|Interfingers with Watchie Sandstone. Age: ~22.5-13.5Ma. Thickness: 15m. Geological region: Billa Kalina area.||||||27-AUG-18
11961|Mirikata Formation|64696|5|Briefly described|p133 Fig.13,Fig.14, |Miocene|Miocene||||Includes the Danae Conglomerate, Millers Creek Dolomite, Billa Kalina Clay, and Watchie Sandstone, Members.|||
11961|Mirikata Formation|66131|6|Mentioned|p242 Fig.2|Miocene|Oligocene|Latest Oligocene to Late Miocene in age (from p.242 Fig.2 - stratigraphic correlation chart).||||||
11961|Mirikata Formation|66520|5|Briefly described|p11. |Tertiary|Tertiary|Gawler Craton.|||Includes Millers Creek Dolomite Member and Billa Kalina Clay Member.|||
11961|Mirikata Formation|67462|5|Briefly described|Map legend.|Miocene|Miocene|Billa Kalina Basin.|||Includes Danae Conglomerate, Billa Kalina Clay, and Millers Creek Dolomite Members.|||
11961|Mirikata Formation|68715|6|Mentioned|p30 Fig.5|Tortonian|Burdigalian|Billa Kalina Basin.||||||
11977|Mitcham Quartzite|22510|5|Briefly described|p36|||Base of Belair Subgroup. Age: Sturtian||||||
11977|Mitcham Quartzite|22889|6|Mentioned|p35|Adelaidean|Adelaidean|Preiss et al., (1993) correlated the Mitcham Quartzite with the Gilbert Range Quartzite but recent mapping suggests that the Mitcham Quartzite actually correlates with the Leasingham Quartzite (now known as the Leasingham Quartzite Member).||||||
11977|Mitcham Quartzite|23818|6|Mentioned|p62|Adelaidean|Adelaidean|Of the Belair Sub-Group.||||||18-APR-05
11977|Mitcham Quartzite|30801|6|Mentioned|p5|||Table P5-6||||||
11977|Mitcham Quartzite|30807|6|Mentioned|p103|||Suggested map symbol||||||
11977|Mitcham Quartzite|33577|6|Mentioned|p80|||Geol. map. Shale deposits P79.||||||
11977|Mitcham Quartzite|34534|6|Mentioned|p57|||Sturtian||||||
11977|Mitcham Quartzite|34535|6|Mentioned|p62|||See Fig.19  Belair Sub.-Gp.||||||
11977|Mitcham Quartzite|34536|6|Mentioned|Map legend|Precambrian|Precambrian|Sturtian||||||
11977|Mitcham Quartzite|36625|6|Mentioned|Fig.1|||||||||
11977|Mitcham Quartzite|39344|6|Mentioned|Map legend|Precambrian|Precambrian|Sturtian||||||
11977|Mitcham Quartzite|39351|6|Mentioned|Map legend|Precambrian|Precambrian|Sturtian||||||
11977|Mitcham Quartzite|40442|5|Briefly described|Fig.4|||||||||
11977|Mitcham Quartzite|41401|6|Mentioned|p29|||||||||
11977|Mitcham Quartzite|41404|4|Described|p118|||||||||
11977|Mitcham Quartzite|41526|6|Mentioned|p47|||||||||
11977|Mitcham Quartzite|42222|6|Mentioned|p15|||||||||
11977|Mitcham Quartzite|42733|6|Mentioned|map legend|Adelaidean||||||||
11977|Mitcham Quartzite|43052|5|Briefly described|p183,Table 6.1|||of Belair Subgroup||||||
11977|Mitcham Quartzite|71237|14|Not recorded|p9|||||||||
11977|Mitcham Quartzite|71529|14|Not recorded|p1, 2|||Previously or alternatively "Glen Osmond Arkosic Quartzite"?||||||
11977|Mitcham Quartzite|72450|5|Briefly described|Brochure map|||||Burra Group|||Massive, coarse-grained, feldspathic quartzite.|
11977|Mitcham Quartzite|73059|6|Mentioned|p1061|||Contains detrital zircons sourced from the adjacent Gawler Craton.||||||
11977|Mitcham Quartzite|73188|5|Briefly described|p325, p329|Neoproterozoic|Neoproterozoic|||Belair Subgroup, Burra Group||||
11977|Mitcham Quartzite|73264|6|Mentioned|p1386, p1387 Fig.10|||Adelaide Rift Complex. Major ziron peaks in the range 1400-1900 Ma, secondary peaks at ~900-1250 Ma.||||||
11977|Mitcham Quartzite|74367|5|Briefly described|p7 Fig.6, p8-9, p11, p14-15, p20|Tonian|Tonian||1053+/-53 Ma LA-ICP-MS detrital zircon MDA|Belair Subgroup||||
11999|Mocamboro Member|24551|6|Mentioned|p247|||At Killara Bluff in the Casterton area. Name proposed to be abandoned by Duddy (1983). Equivalent to Eumeralla Formation.||||||12-JAN-10
11999|Mocamboro Member|30905|4|Described|p148|||||||||
11999|Mocamboro Member|31920|5|Briefly described|p49|||Merino Gp.||||||
11999|Mocamboro Member|34148|6|Mentioned|p272|||||||||
11999|Mocamboro Member|41642|5|Briefly described|Table 7.2|||||||||
11999|Mocamboro Member|42318|6|Mentioned|Fig.5 P12|||||||||
11999|Mocamboro Member|42827|5|Briefly described|Table 7.2|||see also Table 7.3||||||
12040|Molineaux Sand|22857|5|Briefly described|p354|Quaternary|Quaternary|Geological Province: Murray Basin.||||||
12040|Molineaux Sand|23089|6|Mentioned|p649|||||||||
12040|Molineaux Sand|23560|5|Briefly described|p150|||Referred to as Lowan Sand in Vic.||||||
12040|Molineaux Sand|23818|5|Briefly described|p212 Fig.108|Recent|Recent|Geological Province: Murray Basin and Otway Basin. Yellow in colour.||||||27-OCT-08
12040|Molineaux Sand|29697|5|Briefly described|Table 3|||||||||
12040|Molineaux Sand|29829|6|Mentioned|p178|||||||||
12040|Molineaux Sand|30750|6|Mentioned|p4|||||||||
12040|Molineaux Sand|30751|6|Mentioned|Map legend|Recent|Recent|||||||
12040|Molineaux Sand|30752|6|Mentioned|p2|||||||||
12040|Molineaux Sand|30754|2|Defined|Appendix 1|Recent|Recent|Section on p28.||||||27-OCT-08
12040|Molineaux Sand|30755|6|Mentioned|p169|||Tectonic map||||||
12040|Molineaux Sand|30758|6|Mentioned|p66|||Aeolian. Source of fine aggregate P67||||||01-JUL-13
12040|Molineaux Sand|30807|6|Mentioned|p101|||Suggested map symbol||||||
12040|Molineaux Sand|30996|6|Mentioned|p48|||Time equivalent of Coonambidgal Formation.||||||27-OCT-08
12040|Molineaux Sand|31241|6|Mentioned|p97|||Geological map||||||
12040|Molineaux Sand|31625|6|Mentioned|Fig. 5.2|||Pleistocene||||||
12040|Molineaux Sand|32323|6|Mentioned|p9|||Recent, aeolian.||||||
12040|Molineaux Sand|32432|6|Mentioned|Fig.2|||See also Table 1||||||
12040|Molineaux Sand|32433|6|Mentioned|p80|||See also Table 2||||||
12040|Molineaux Sand|32438|6|Mentioned|p42|||||||||
12040|Molineaux Sand|32439|6|Mentioned|p99|||||||||
12040|Molineaux Sand|33767|6|Mentioned|Fig.5|||||||||
12040|Molineaux Sand|34180|6|Mentioned|p212|||Recent. See also p217.||||||27-OCT-08
12040|Molineaux Sand|34191|6|Mentioned|Map legend|Pleistocene|Pleistocene|Pleistocene - Recent||||||
12040|Molineaux Sand|34536|6|Mentioned|Map legend|Recent|Recent|||||||
12040|Molineaux Sand|35071|6|Mentioned|Table 1|||||||||
12040|Molineaux Sand|35097|6|Mentioned|Fig.4|||||||||
12040|Molineaux Sand|35272|6|Mentioned|p285|||||||||
12040|Molineaux Sand|35772|6|Mentioned|p14|||||||||
12040|Molineaux Sand|36621|6|Mentioned|Fig.1|||||||||
12040|Molineaux Sand|36623|6|Mentioned|Fig.1|||||||||
12040|Molineaux Sand|38068|6|Mentioned|Fig.8|||||||||
12040|Molineaux Sand|40003|5|Briefly described|Table 10|||See also Table 11||||||
12040|Molineaux Sand|40230|6|Mentioned|p6|||||||||
12040|Molineaux Sand|41848|6|Mentioned|p360|||Part equivalent to Lowan Sand||||||
12040|Molineaux Sand|42125|6|Mentioned|p139|||||||||
12040|Molineaux Sand|42129|6|Mentioned|Table 1 P253|||||||||
12040|Molineaux Sand|42499|6|Mentioned|Map legend|||||||||
12040|Molineaux Sand|42717|5|Briefly described|map legend|Holocene||||||||
12040|Molineaux Sand|42966|1|Redefined|p270|Holocene|Late Pleistocene|||||||
12040|Molineaux Sand|43073|4|Described|p18,Table 4|||||||||
12040|Molineaux Sand|43195|5|Briefly described|Map Legend|Holocene|Late Pleistocene|see also commentary on back of map.||||||
12040|Molineaux Sand|44133|5|Briefly described|p220 Fig. 11.2, 253|Holocene|Middle Pleistocene|Equivalent to the Lowan Sand. Geological Province: Murray Basin.||||||
12040|Molineaux Sand|44660|14|Not recorded|map legend|||Recent.||||||
12040|Molineaux Sand|49038|4|Described|Table 2|||Briefly described p32.||||||27-OCT-08
12040|Molineaux Sand|50154|6|Mentioned|p140|||Equivalent to the Lowan Sand||||||
12040|Molineaux Sand|61964|6|Mentioned|p170|||Noted by Brown and Stephenson (1991a) that this unit in SA and the Lowan Sand of Victoria are essentially the same unit.||||||
12040|Molineaux Sand|63124|6|Mentioned|p93|||Geological Province: Gambier Basin.||||||
12040|Molineaux Sand|65715|6|Mentioned|p25 Fig.1a|||Map symbol implies Quarternary age.||||||
12040|Molineaux Sand|68116|5|Briefly described|Appendix and many maps (see Comments). |Holocene|Pleistocene|Maps  3-4, 6-7, 9-11, 14-15, 21-22, 29-30, 38-39, 47-48.|||||Aeolian dune sand, fine to medium grained; quartz-rich and clay-poor.|
12040|Molineaux Sand|70334|6|Mentioned|p69|||Of Murray Basin.||||||
12040|Molineaux Sand|71129|6|Mentioned|p155|Pleistocene|Pleistocene|Of Murray Basin. Equivalent to Pleistocene aeolian sand sheets in SIX MILE HILL.||||||
12040|Molineaux Sand|71593|5|Briefly described|p56|||Formed from wind-blown Loxton Sand sediment.|||||Windblown sand dune fields.|
12040|Molineaux Sand|73112|5|Briefly described|Map legend.|Holocene|Holocene|Age given is Recent.|||||Off-white, pale yellow-brown or orange sand of the inland dune spread.|
12040|Molineaux Sand|73228|6|Mentioned|p53|||Fluvio-aeolian depositional environment. Identified in Nadda 1 drillhole.||||Underlain by Loxton Sand.|Red to white, fine to coarse sands.|
12073|Monarto Granite|9124|5|Briefly described|Map Legend|Paleozoic|Paleozoic|Light grey, fine-grained, even-grained adamellite, occasionally gneissic.||||||07-NOV-08
12073|Monarto Granite|24361|6|Mentioned|p50, Fig. 1b|||||||||
12073|Monarto Granite|24509|6|Mentioned|p39 Fig. 1, p40, p42 Tb. 1|||I-type granite. Geological Province: Adelaide Geosyncline.||||||04-MAY-05
12073|Monarto Granite|29406|6|Mentioned|p52|||||||||
12073|Monarto Granite|29697|6|Mentioned|Fig.39|||||||||
12073|Monarto Granite|30753|6|Mentioned|p12|||Refers Blissett (1970)||||||
12073|Monarto Granite|30758|5|Briefly described|p66|||Genesis in situ. Early Ordovician,Delamerian. Aggregate||||||
12073|Monarto Granite|31851|6|Mentioned|p10|||||||||
12073|Monarto Granite|32432|6|Mentioned|Fig.2|||See also Table 1||||||
12073|Monarto Granite|40442|6|Mentioned|p18|||||||||
12073|Monarto Granite|42093|6|Mentioned|p8|||||||||
12073|Monarto Granite|42271|5|Briefly described|p384|||||||||
12073|Monarto Granite|42275|6|Mentioned|Table 1 P470|||||||||
12073|Monarto Granite|42884|5|Briefly described|Fig.1 P11|||||||||
12073|Monarto Granite|43190|6|Mentioned|Fig.1,p28.|||||||||
12073|Monarto Granite|44133|5|Briefly described|p56 Table 7.3|||Foliated fine grained adamellite. Undated. Age referred as possibly syn-DD2 (?earliest Ordovician)||||||28-SEP-12
12073|Monarto Granite|61307|6|Mentioned|p12|||||||||
12073|Monarto Granite|61525|6|Mentioned|p40|||||||||
12073|Monarto Granite|64769|6|Mentioned|p28|Paleoproterozoic|Paleoproterozoic|Light grey in colour. SA.||||||28-SEP-12
12073|Monarto Granite|68314|6|Mentioned|p755 Fig.6|Middle Cambrian|Middle Cambrian|Age inferred from Fig.6.|501 +/- 3 Ma (Foden et al., 2004).|||||
12109|Monoman Formation|23818|5|Briefly described|p212 Fig.108|Recent|Recent|Geological Province: Murray Basin.||||||
12109|Monoman Formation|30750|6|Mentioned|p3|||||||||
12109|Monoman Formation|30751|6|Mentioned|Map legend|Recent|Recent|||||||
12109|Monoman Formation|30753|4|Described|p14|||Recent age||||||
12109|Monoman Formation|30754|2|Defined|Appendix 1|Recent|Recent|||||||
12109|Monoman Formation|30996|3|Fully described|p45|||Refers Firman (1971). L. Holocene - Uppermost Pleistocene.||||||
12109|Monoman Formation|32007|4|Described|p161|||Late Pleistocene. Fossils discussed||||||
12109|Monoman Formation|32426|6|Mentioned|p142|||Stratigraphic table. Renmark area||||||
12109|Monoman Formation|34180|6|Mentioned|p212|||Recent||||||
12109|Monoman Formation|34758|6|Mentioned|p27|||||||||
12109|Monoman Formation|35071|6|Mentioned|Fig.4|||||||||
12109|Monoman Formation|35097|6|Mentioned|Fig.4|||||||||
12109|Monoman Formation|35174|6|Mentioned|p167|||||||||
12109|Monoman Formation|35200|6|Mentioned|Map legend|Holocene|Holocene|||||||
12109|Monoman Formation|35232|6|Mentioned|Table.4|||||||||
12109|Monoman Formation|35272|6|Mentioned|p280|||||||||
12109|Monoman Formation|38383|6|Mentioned|Table 1|||||||||
12109|Monoman Formation|41848|5|Briefly described|p356|||Old subdivision at base of Coonambidgal Formation, not used in this book||||||07-APR-17
12109|Monoman Formation|42128|5|Briefly described|p227|||See also Fig.2||||||
12109|Monoman Formation|42264|4|Described|p9|||See also Fig.3||||||
12109|Monoman Formation|42827|5|Briefly described|p356|||||||||
12109|Monoman Formation|42966|1|Redefined|Table 39 p278|Holocene|Late Pleistocene|||||||
12109|Monoman Formation|43655|5|Briefly described|p40-846|||||||||
12109|Monoman Formation|44133|6|Mentioned|p254 Fig. 11.28|Holocene|Holocene|||||||
12109|Monoman Formation|61155|5|Briefly described|p18|Pleistocene|Pleistocene|Geological Province: Murray Basin.||||||
12109|Monoman Formation|68716|6|Mentioned|p39 Fig.3, p40, p41|||A source of lateral flow, saline groundwater discharges to the Murray River.||||Overlain by the Coonambidgal Formation. Underlain by the Bookpurnong Formation.||07-APR-17
12109|Monoman Formation|73188|6|Mentioned|p320|Holocene|Holocene|Murray Basin.|||||Sand, clay, gravel, loam.|
12170|Mooga Sandstone|730|6|Mentioned|p24.|||Fluviatile.||||||11-NOV-14
12170|Mooga Sandstone|12597|5|Briefly described|p492 Tb.1, p495 Fig.3, p497|Early Cretaceous|Early Cretaceous|N Surat Basin. 50-100m thick. Basal section is permeable and acts as a major aquifer.||||Grades laterally into upper part of Hooray Sandstone.|Quartzose, sub-labile, upward-fining fluvial sandstone, with interbeds of siltstone and mudstone at the top.|
12170|Mooga Sandstone|13516|6|Mentioned|p167 fig 10, p169 fig 11|Early Cretaceous|Early Cretaceous|In Surat Basin, Eromanga Basin.||||||
12170|Mooga Sandstone|22757|5|Briefly described|Table6,p11||Early Cretaceous|60 m. Surat Basin.||||||
12170|Mooga Sandstone|22857|4|Described|p295, p296-7 Tb.22.1, p546 Tb.A1.12|Hauterivian|Berriasian|Of the Blythesdale Group. Fine-grained sublabile to quartzose arenite with interbedded siltstone and shale. Equivalent of Hooray Sandstone (Eromanga Basin). Max. thickness: 56m. Geological Province: Surat Basin. See also p312-3 Fig. 22.6, p314-5.||||||
12170|Mooga Sandstone|22865|4|Described|p295,Table22.1p296-7|Valanginian|Berriasian|||||||
12170|Mooga Sandstone|23053|6|Mentioned|Fig10p17,26|Valanginian|Tithonian|||||||
12170|Mooga Sandstone|23056|6|Mentioned|9|||Geol province Eromanga Basin||||||
12170|Mooga Sandstone|23818|6|Mentioned|140|Triassic|Triassic|Geological Province: Great Artesian Basin.||||||
12170|Mooga Sandstone|23911|5|Briefly described|p96 Fig. 10, p97 Fig. 11|Cretaceous|Cretaceous|Geological Province: Surat Basin.||||||
12170|Mooga Sandstone|23982|5|Briefly described|p58 Fig.18|||Geological Province: Surat Basin.||||||
12170|Mooga Sandstone|24068|4|Described|p270 Table 2|Early Cretaceous|Early Cretaceous|Geological Province: Surat Basin.  Maximum thickness: 140m.||||||
12170|Mooga Sandstone|24070|5|Briefly described|p303|Late Jurassic|Middle Jurassic|Geological Province: Coonamble Embayment.||||||
12170|Mooga Sandstone|24092|5|Briefly described|p8 Fig.3|||Geological Province: Surat Basin.||||||
12170|Mooga Sandstone|29379|6|Mentioned|Fig.11|||Showing oil company usage compared with Freytag(1966)&Forbes(1966).||||||
12170|Mooga Sandstone|29387|6|Mentioned|Table 5|||||||||
12170|Mooga Sandstone|29393|6|Mentioned|Table 4|||||||||
12170|Mooga Sandstone|29591|6|Mentioned|p77|||||||||
12170|Mooga Sandstone|29721|6|Mentioned|Table 246|||||||||
12170|Mooga Sandstone|30021|6|Mentioned|p87|||||||||
12170|Mooga Sandstone|30022|6|Mentioned|p28|||||||||
12170|Mooga Sandstone|30024|6|Mentioned|p332|||||||||
12170|Mooga Sandstone|30540|6|Mentioned|Fig.6|||||||||
12170|Mooga Sandstone|30692|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|||||||
12170|Mooga Sandstone|30694|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
12170|Mooga Sandstone|30695|4|Described|Table 4|||Lower Cretaceous age||||||
12170|Mooga Sandstone|30696|4|Described|Table 4|||Lower Cretaceous age||||||
12170|Mooga Sandstone|30697|6|Mentioned|p34|||Major aquifer present||||||
12170|Mooga Sandstone|30698|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
12170|Mooga Sandstone|30699|6|Mentioned|p53|||Middle Jurassic - Early Cretaceous. Stratigraphy||||||
12170|Mooga Sandstone|30701|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
12170|Mooga Sandstone|30702|4|Described|p48|||See also p49-51, Table 1, Fig.1,2.||||||13-JUN-22
12170|Mooga Sandstone|30914|6|Mentioned|Map legend|Cretaceous|Jurassic|Jurassic - Cretaceous||||||
12170|Mooga Sandstone|31097|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
12170|Mooga Sandstone|31098|5|Briefly described|Table 1|||Lower Cretaceous||||||
12170|Mooga Sandstone|31116|4|Described|p40|||Cretaceous. See also Table 2||||||
12170|Mooga Sandstone|31369|6|Mentioned|Table 4|||Cretaceous||||||
12170|Mooga Sandstone|31376|6|Mentioned|p4|||||||||
12170|Mooga Sandstone|32193|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
12170|Mooga Sandstone|32276|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
12170|Mooga Sandstone|32797|4|Described|Table 4|||L.Cret.||||||
12170|Mooga Sandstone|33070|4|Described|Table 2|||L.Cret.||||||
12170|Mooga Sandstone|33071|6|Mentioned|p6|||L.Cret.||||||
12170|Mooga Sandstone|33075|6|Mentioned|p451|||||||||
12170|Mooga Sandstone|33080|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
12170|Mooga Sandstone|33090|4|Described|Table 4|||L.Cret.||||||
12170|Mooga Sandstone|33091|5|Briefly described|p7|||Stratigraphy||||||
12170|Mooga Sandstone|33094|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
12170|Mooga Sandstone|33165|6|Mentioned|Chart|||Correlation chart only||||||
12170|Mooga Sandstone|33367|6|Mentioned|p17|||||||||
12170|Mooga Sandstone|33414|6|Mentioned|p214|||||||||
12170|Mooga Sandstone|33451|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
12170|Mooga Sandstone|33523|6|Mentioned|p27|||||||||
12170|Mooga Sandstone|33672|6|Mentioned|p44|||||||||
12170|Mooga Sandstone|33828|6|Mentioned|Table 3|||||||||
12170|Mooga Sandstone|33939|6|Mentioned|p412|||Blythesdale Group.||||||
12170|Mooga Sandstone|33971|6|Mentioned|Fig.29|||Strat. table.||||||
12170|Mooga Sandstone|34254|6|Mentioned|p491|||||||||
12170|Mooga Sandstone|34543|6|Mentioned|p98|||||||||
12170|Mooga Sandstone|34611|6|Mentioned|p140|||Jurassic. Correlation chart. Fig.65.||||||
12170|Mooga Sandstone|34613|4|Described|Table 4|||||||||
12170|Mooga Sandstone|35793|6|Mentioned|Fig.3|||||||||
12170|Mooga Sandstone|35937|6|Mentioned|Fig.5|||||||||
12170|Mooga Sandstone|36243|6|Mentioned|Table 7A|||||||||
12170|Mooga Sandstone|36570|4|Described|p49|||See also p45, Fig.9, p60.||||||13-JUN-22
12170|Mooga Sandstone|36751|6|Mentioned|p488|||||||||
12170|Mooga Sandstone|36827|6|Mentioned|p83|||||||||
12170|Mooga Sandstone|37117|5|Briefly described|p313|||||||||
12170|Mooga Sandstone|37995|4|Described|p65|||||||||
12170|Mooga Sandstone|38068|6|Mentioned|p71|||||||||
12170|Mooga Sandstone|39211|5|Briefly described|p31|||See also Fig.3||||||
12170|Mooga Sandstone|39212|5|Briefly described|p17|||Early Neocomian. See also p15.||||||13-JUN-22
12170|Mooga Sandstone|39215|6|Mentioned|p51|||Spore/pollen record||||||
12170|Mooga Sandstone|39218|6|Mentioned|p48|||Flora||||||
12170|Mooga Sandstone|39315|6|Mentioned|Fig.5|||||||||
12170|Mooga Sandstone|39445|5|Briefly described|Table 10|||||||||
12170|Mooga Sandstone|39494|6|Mentioned|Fig.5|||||||||
12170|Mooga Sandstone|39914|6|Mentioned|p2|||||||||
12170|Mooga Sandstone|39943|6|Mentioned|Table 9A|||||||||
12170|Mooga Sandstone|39998|6|Mentioned|p192|||||||||
12170|Mooga Sandstone|40030|6|Mentioned|Fig.5|||||||||
12170|Mooga Sandstone|40245|6|Mentioned|Table 2|||||||||
12170|Mooga Sandstone|40249|6|Mentioned|p38|||Mention P41||||||
12170|Mooga Sandstone|40250|6|Mentioned|Fig.1|||||||||
12170|Mooga Sandstone|40541|3|Fully described|p110|||||||||
12170|Mooga Sandstone|40544|6|Mentioned|Fig.6|||||||||
12170|Mooga Sandstone|40666|4|Described|p358|||||||||
12170|Mooga Sandstone|40675|6|Mentioned|Table 9A|||||||||
12170|Mooga Sandstone|40687|6|Mentioned|p417|||||||||
12170|Mooga Sandstone|40926|6|Mentioned|p13|||||||||
12170|Mooga Sandstone|41057|6|Mentioned|p61|||||||||
12170|Mooga Sandstone|41060|6|Mentioned|Fig.3|||||||||
12170|Mooga Sandstone|41061|6|Mentioned|Fig.6|||||||||
12170|Mooga Sandstone|41064|6|Mentioned|p60|||||||||
12170|Mooga Sandstone|41187|6|Mentioned|Fig.2|||||||||
12170|Mooga Sandstone|41188|6|Mentioned|Fig.3|||||||||
12170|Mooga Sandstone|41210|5|Briefly described|Fig.3|||||||||
12170|Mooga Sandstone|41216|6|Mentioned|Fig.18|||||||||
12170|Mooga Sandstone|41246|6|Mentioned|Map legend|Cretaceous|Jurassic|||||||
12170|Mooga Sandstone|41247|6|Mentioned|Fig.7|||||||||
12170|Mooga Sandstone|41266|6|Mentioned|Fig.3|||||||||
12170|Mooga Sandstone|41681|6|Mentioned|p16|||||||||
12170|Mooga Sandstone|41712|6|Mentioned|p282|||||||||
12170|Mooga Sandstone|41992|4|Described|Fig.2 P183|||||||||
12170|Mooga Sandstone|42007|5|Briefly described|Fig.2 P182|||||||||
12170|Mooga Sandstone|42135|6|Mentioned|Fig.6 P357|||||||||
12170|Mooga Sandstone|42493|5|Briefly described|Fig. 1 P18|||||||||
12170|Mooga Sandstone|42494|5|Briefly described|Table 1 P24|||||||||
12170|Mooga Sandstone|42634|6|Mentioned|Table 8 P34|||||||||
12170|Mooga Sandstone|43000|5|Briefly described|Fig.5,p112|||Of Blythesdale Group.||||||16-SEP-08
12170|Mooga Sandstone|43002|5|Briefly described|Fig.2,p135|||||||||
12170|Mooga Sandstone|43404|14|Not recorded|Table p11|Cretaceous|Jurassic|||||||
12170|Mooga Sandstone|43602|6|Mentioned|Fig3 p194|||In Surat Basin, Blythesdale Group.  Misspelling of Mooga Formation?||||||
12170|Mooga Sandstone|43883|14|Not recorded|p18 Fig.4-3|||||||||
12170|Mooga Sandstone|43991|5|Briefly described|p50|Cretaceous|Jurassic|Part of the "Blythesdale Group".||||||
12170|Mooga Sandstone|43995|14|Not recorded|p13,57,58,Fig.5|||Part of Blythesdale Group.||||||
12170|Mooga Sandstone|44021|14|Not recorded|p233,238|||Equivalent to "Hooray Sandstone" in Eromanga Basin.||||||
12170|Mooga Sandstone|44087|14|Not recorded|p6|||Equivalent to part of Blythesdale Group on Betoota sheet.||||||
12170|Mooga Sandstone|44088|4|Described|p6|||Equivalent to part of Blythesdale Group on Betoota sheet.||||||
12170|Mooga Sandstone|44091|14|Not recorded|p60||Cretaceous|||||||
12170|Mooga Sandstone|44171|14|Not recorded|p194|||||||||
12170|Mooga Sandstone|44375|14|Not recorded|p310,311|||Aquifer.||||||
12170|Mooga Sandstone|44377|1|Redefined|p2,7-11,15|||Redefined as Mooga Sandstone Member. Of Blythesdale Formation.||||||
12170|Mooga Sandstone|44915|14|Not recorded|p18|||Ref. to Day 1964, Whitehouse 1955, Vine and Day 1965. Equivalent to Village Well Formation in South Australia. No age given.||||||
12170|Mooga Sandstone|45103|6|Mentioned|p6|||||||||
12170|Mooga Sandstone|45110|2|Defined|p105|Early Cretaceous|Early Cretaceous|See also p9 and p24.||||||13-JUN-22
12170|Mooga Sandstone|45132|6|Mentioned|Table 2|||See also Fig.1.||||||
12170|Mooga Sandstone|46791|5|Briefly described|p42|||||||||
12170|Mooga Sandstone|46937|5|Briefly described|Fig.10|||See also Table 1.||||||
12170|Mooga Sandstone|46984|6|Mentioned|Table 1|||||||||
12170|Mooga Sandstone|48634|14|Not recorded|p6,20||Late Jurassic|See also Fig.2,6, Pl.1,2 p5,19. Upper Jurassic. (G54-14).||||||
12170|Mooga Sandstone|48919|4|Described|p70|||See also Table 5||||||
12170|Mooga Sandstone|48920|6|Mentioned|Table 7|||Refers Exon & Vine (1970)||||||
12170|Mooga Sandstone|49010|6|Mentioned|Fig.4|||Surat Basin||||||
12170|Mooga Sandstone|49011|6|Mentioned|Fig.3|||Surat Basin||||||
12170|Mooga Sandstone|61611|6|Mentioned|p265 Fig. 3|Late Jurassic|Early Cretaceous|Geological Province: Surat Basin.||||||13-MAR-09
12170|Mooga Sandstone|63218|6|Mentioned|p211 Fig.2. |Early Cretaceous|Early Cretaceous|Surat Basin.||||||
12170|Mooga Sandstone|63979|5|Briefly described|p40, p44|Late Jurassic|Late Jurassic|Geological province: Surat Basin.||||||07-FEB-11
12170|Mooga Sandstone|64197|6|Mentioned|p630 Fig.7|Early Cretaceous|Early Cretaceous|||||Underlies Bungil Formation; overlies Orallo Formation.||
12170|Mooga Sandstone|64665|5|Briefly described|p53 Fig.2, p62.|Early Cretaceous|Early Cretaceous|Surat Basin.||||Overlies Orallo Formation. Is overlain by Bungil Formation.||
12170|Mooga Sandstone|64856|3|Fully described|p79, p95-98|Valanginian|Berriasian|Surat Basin. Of Reeves (1947). Renamed Mooga Sandstone Member (of Blythesdale Formation) by Day (1964), with a type area along Blyth Creek, 24-34km ENE of Roma. Renamed back to Mooga Sandstone by Exon and Vine (1970) with a new type area near the junction of Bungil and Mooga-Mooga Creeks, 16km N of Roma. Overlies Orallo Formation conformably, locally disconformably. Grades into upper Hooray Sandstone to the west. Is overlain conformably by Bungil Formation. Age from palynofloral units APK1, 21. <168m. Sublabile to quartzose sandstone, minor siltstone.|| ||||29-NOV-17
12170|Mooga Sandstone|64857|5|Briefly described|p113 Fig.3, p115|||Overlies Orallo Formation, Surat Basin.||||||
12170|Mooga Sandstone|64858|6|Mentioned|p187-188|||See also Mooga Formation.||||||16-MAR-12
12170|Mooga Sandstone|65003|4|Described|p1,p13, p14, p25|Cretaceous|Cretaceous|||||Overlies the Orallo Formation and the Boondooma Igneous Complex|Fine to medium-grained fawn sandstone that weathers yellow and brown.|
12170|Mooga Sandstone|65112|6|Mentioned|Fig 11 p324|Early Cretaceous|Early Cretaceous|Unit in the Surat Basin. Underlies the Bungil Formation, overlies the Orallo Formation.||||||22-MAR-12
12170|Mooga Sandstone|65113|5|Briefly described|Fig 4 p340|Early Cretaceous|Early Cretaceous|Overlies the Orallo Formation, underlies the Bungil Formation.||||||
12170|Mooga Sandstone|65114|5|Briefly described|p385 Fig.3|Early Cretaceous||||||||
12170|Mooga Sandstone|65116|5|Briefly described|p456, Fig 2 p437|Early Cretaceous|Early Cretaceous|Underlies the Bungil Formation, Overlies the Orallo Formation, Surat Basin.||||||
12170|Mooga Sandstone|65119|5|Briefly described|Fig 2 p503, Fig 7- 8, 14, 16-19|Early Cretaceous |Early Cretaceous|Surat Basin. Quartzose to lithic sandstone, some mud and siltstone, up to 300m thick.||||||
12170|Mooga Sandstone|66529|6|Mentioned|p12 Fig.5 |||Surat Basin.||||Overlies Orallo Formation. Is overlain by Bungil Formation.||
12170|Mooga Sandstone|66915|5|Briefly described|p6 Fig.3, p9, p11 Fig.7|Early Cretaceous|Early Cretaceous|Surat Basin.||||||12-JAN-17
12170|Mooga Sandstone|67133|5|Briefly described|p17, p21|Cretaceous|Cretaceous|Not included in this study. Part of the final cycle of deposition under fluvial conditions in the Surat Basin.||||Overlies Orallo Formation. Is overlain by Bungil Formation.||
12170|Mooga Sandstone|67402|4|Described|p146 fig SRT3, p148, p156|Barremian|Tithonian|Surat Basin. Deposited in a braided or meandering fluvial environment. Approximately 178m thick.||Blythesdale Group||Overlies the Orallo Formation. Overlain by the Bungil Formation.|Sandstone, minor clay, siltstone and mudstone.|
12170|Mooga Sandstone|67669|5|Briefly described|p11|Early Cretaceous|Early Cretaceous|Of Bowen Basin.||Unit of Blythesdale Group.||Overlain by Bungil Formation. Underlain by Orallo Formation.||
12170|Mooga Sandstone|68003|5|Briefly described|p52, p56, p57 Fig.3-n.|Early Cretaceous|Early Cretaceous|Surat Basin. Equivalent to part of Keelindi beds.||Unit in Blythesdale Group.||Overlies Orallo Formation. Is overlain by Bungil Formation.||
12170|Mooga Sandstone|68004|6|Mentioned|p174, p175.|||Major aquifer for water production; excellent quality reservoir. Sealed by Wallumbilla Formation shales. A major hydrocarbon exploration target. See also reference to Mooga Formation p87.||||||
12170|Mooga Sandstone|68069|5|Briefly described|Map legend.|Early Cretaceous|Early Cretaceous|Surat Basin. Shown on cross-sections and time-space plot and basement interpretation only. Fluvial environment.||||Overlies Orallo Formation. Is overlain by Bungil Formation.|Quartzose, sub-labile sandstone; minor siltstone, shale, mudstone and coal.|
12170|Mooga Sandstone|68117|6|Mentioned|p346|Early Cretaceous|Early Cretaceous|Surat Basin.||||||
12170|Mooga Sandstone|68135|5|Briefly described|p52 fig 2b|Early Cretaceous|Early Cretaceous|Surat Basin (NSW and QLD): contains plant macrofossils in the latter.||||Overlies Orallo Formation|Silty sandstone.|14-SEP-17
12170|Mooga Sandstone|68139|6|Mentioned|p23|Early Cretaceous|Early Cretaceous|Surat Basin.||||Overlies Orallo Formation. Is overlain by Bungil Formation.||
12170|Mooga Sandstone|68553|6|Mentioned|Map legend; schematic diagram.|Early Cretaceous|Jurassic|Surat Basin. This unit, as well as Bungil, Orallo and Southlands Formations; Gubberamunda, Hooray and Longsight Sandstones, and Kumbarilla beds, are all mapped under the symbol, JKb.||||||
12170|Mooga Sandstone|68576|5|Briefly described|Q_4: p3|Early Cretaceous|Early Cretaceous|Surat Basin.||||Overlies Orallo Formation. Is overlain by Bungil Formation.||
12170|Mooga Sandstone|68593|5|Briefly described|p3-4, p45, p47|Early Cretaceous|Early Cretaceous|Fluvial deposits. One of the main artesian aquifers in the map area.||||Overlies Orallo Formation. Is overlain by Bungil Formation.|Quartzose, sub-labile sandstone, minor siltstone, shale, mudstone and coal.|
12170|Mooga Sandstone|68734|6|Mentioned|p218 Fig.2, p221 Fig.3|||Surat Basin. Fluvial. Pre-Barremian age.||||||16-JAN-17
12170|Mooga Sandstone|69582|6|Mentioned|p36|Early Cretaceous|Early Cretaceous|Surat Basin.||||Overlies the Orallo Formation. Overlain by the Bungil Formation.||
12170|Mooga Sandstone|69594|5|Briefly described|p519, p527, p537-538, p573|Hauterivian|Valanginian|Reeves (1947); Exon and Vine (1970). Northern Surat Basin. Braided to meandering stream deposits. Up to 168m thick. An important local aquifer in the Roma district.||||Conformably overlies Orallo Formation, locally disconformably. Is overlain conformably by Bungil Formation. Equivalent to/laterally grades into Hooray Sandstone and Kumbarilla beds.|Three subunits: a lower sublabile to quartzose sandstone that is commonly conglomeratic; a middle mudstone; and an upper subunit of interbedded fine sublabile sandstone and siltstone.|
12170|Mooga Sandstone|69681|6|Mentioned|p74 Fig.3|Early Cretaceous|Early Cretaceous|Mineralogy and likely chemical changes from CO2 injection discussed.||||||
12170|Mooga Sandstone|69790|6|Mentioned|p1063 Fig.2|Cretaceous|Cretaceous|Northern Surat Basin.||||||
12170|Mooga Sandstone|70036|5|Briefly described|Map legend|||Surat Basin. Included in a mapped unit of a Late Jurassic to Early Cretaceous meandering stream sequence: quartzose sandstone and conglomerate with minor shale, mudstone and coal.||||||
12170|Mooga Sandstone|70821|5|Briefly described|p21 Fig.2.6, p22 Fig.2.7, p33, p80|Early Cretaceous|Jurassic|Surat Basin.  Aquifer: generally artesian. Appears as Mooga Sandstone Member in Fig.2.6.||||Overlies Walloon Coal Measures and Orallo Formation. Is overlain by Bungil Formation or Cadna-owie Formation.||
12170|Mooga Sandstone|70836|6|Mentioned|p474|Early Cretaceous|Early Cretaceous|Lightning Ridge area, Surat Basin. Berriasian-Valanginian.||||Overlies Orallo Formation. Is overlain by Bungil Formation.||
12170|Mooga Sandstone|71806|6|Mentioned|p484|Cretaceous|Cretaceous|Surat Basin.||||||
12170|Mooga Sandstone|72298|5|Briefly described|p801|Cretaceous|Cretaceous|Surat Basin (QLD,NSW), Coonamble Embayment (NSW). Main confined aquifers, generally producing flowing artesian water bores.||||Overlies Orallo FZ. Is overlain by Kingull Member (Bungil FZ).||
12170|Mooga Sandstone|72921|5|Briefly described|p15 Fig.2.|Cretaceous|Cretaceous|Shown as located in the Surat Basin, both Qld and NSW.||||Overlies Orallo Formation||
12170|Mooga Sandstone|73113|5|Briefly described|p. 22-24, 36-37, 41, 43, 69, 80, 88...|||Surat Basin. Regional aquifer. More locations: p. 116-117, 119, 146, 151-152, 160, 169-173, 177-178, 191.||||||
12170|Mooga Sandstone|73193|6|Mentioned|p369|Hauterivian|Valanginian|Surat Basin.||||Underlain by Orallo Formation. Overlain by Bungil Formation.||
12195|Moolooloo Siltstone Member|22921|5|Briefly described|38|||Parent Sandison Subgroup||||||
12195|Moolooloo Siltstone Member|23287|6|Mentioned|Fig.3|||Age: Lower Ediacarian. of Sandison Subgroup.||||||
12195|Moolooloo Siltstone Member|24195|5|Briefly described|p45 Fig.3|||Of the Brachina Formation. Geological Province: Adelaide Geosyncline||||||
12195|Moolooloo Siltstone Member|30807|6|Mentioned|p102|||Suggested map symbol||||||
12195|Moolooloo Siltstone Member|34291|6|Mentioned|p19|||Adelaidean. See also P74||||||
12195|Moolooloo Siltstone Member|35586|6|Mentioned|p26|||Now to be known as Moolooloo Formation.||||||
12195|Moolooloo Siltstone Member|37932|5|Briefly described|p546|||||||||
12195|Moolooloo Siltstone Member|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Marinoan||||||
12195|Moolooloo Siltstone Member|41429|5|Briefly described|p120|||||||||
12195|Moolooloo Siltstone Member|42222|6|Mentioned|p19|||||||||
12195|Moolooloo Siltstone Member|42600|6|Mentioned|p9|||of Brachina Fmn||||||
12195|Moolooloo Siltstone Member|43052|5|Briefly described|p192,table 6.1|||Of Brachina Formation.||||||30-SEP-08
12195|Moolooloo Siltstone Member|43622|6|Mentioned|p38|Neoproterozoic||||||||
12195|Moolooloo Siltstone Member|60959|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Of the Brachina Formation. Drab olive-green micaceous siltstone overlying lower red sandstone.||||||
12195|Moolooloo Siltstone Member|61732|5|Briefly described|p28 Fig. 13, p39|Marinoan|Marinoan|Of the Brachina Formation. Extensive red-brown, finely laminated mud and silt. Geological Province: Adelaide Rift Complex.||||||07-FEB-11
12195|Moolooloo Siltstone Member|64455|5|Briefly described|p138 Fig. 1|Cryogenian|Cryogenian|Of Brachina Formation. Overlian by Moorillah Siltstone Member. Green - grey mudstone.||||||29-JAN-09
12195|Moolooloo Siltstone Member|67030|6|Mentioned|p409 Fig. 2|Ediacaran|Ediacaran|||Of Brachina Formation||Overlies the Nuccaleena Formation and Seacliff Sandstone; underlies the Moorillah Siltstone Member.||26-APR-12
12195|Moolooloo Siltstone Member|70334|6|Mentioned|p33|||Geological province: Gawler Craton.||||||
12195|Moolooloo Siltstone Member|70406|5|Briefly described|p122, 121 Fig 5.|Neoproterozoic|Neoproterozoic|||Base of Brachina Formation.||Sharply overlain by Corraberra Sandstone Member. Lateral eqivalent of Tregolana Shale Member.||
12195|Moolooloo Siltstone Member|70407|5|Briefly described|p103 Fig 2|Neoproterozoic|Neoproterozoic|Age: Marinoan.||Of Brachina Formation.||||
12217|Moonabie Formation|22629|4|Described|p152, figs2,4|Statherian|Statherian|||||||
12217|Moonabie Formation|23481|5|Briefly described|p19 Fig 1|||Geological Province: Gawler Craton.||||||
12217|Moonabie Formation|23719|4|Described|p17|Paleoproterozoic|Paleoproterozoic|See also page 14 table 1. Overlain by Corunna Conglomerate. Underlain by McGregor Volcanics. Geol. Province: Gawler Craton.||||||07-NOV-08
12217|Moonabie Formation|23805|5|Briefly described|p4 Fig. 1|Paleoproterozoic|Paleoproterozoic|Geological Province: Gawler Craton.||||||07-NOV-08
12217|Moonabie Formation|23818|5|Briefly described|p30|||Intruded by the Moonabie Porphyry. Geological Province: Gawler Block.||||||
12217|Moonabie Formation|24505|5|Briefly described|p5 Fig. 1|||Geological Province: Gawler Craton.||||||15-SEP-05
12217|Moonabie Formation|30237|6|Mentioned|Fig.1|||||||||
12217|Moonabie Formation|30806|5|Briefly described|Table 1|||||||||
12217|Moonabie Formation|30807|6|Mentioned|p103|||Suggested map symbol||||||
12217|Moonabie Formation|30845|6|Mentioned|Fig.1|||||||||
12217|Moonabie Formation|31034|6|Mentioned|Fig. 2|||||||||
12217|Moonabie Formation|31320|6|Mentioned|p13|||||||||
12217|Moonabie Formation|32458|6|Mentioned|p10|||||||||
12217|Moonabie Formation|32507|6|Mentioned|Table 3|||||||||
12217|Moonabie Formation|33468|6|Mentioned|Fig.6|||Carpentarian. See also P205||||||
12217|Moonabie Formation|33470|4|Described|p463|||||||||
12217|Moonabie Formation|33479|6|Mentioned|Fig.1|||||||||
12217|Moonabie Formation|33557|6|Mentioned|p10|||||||||
12217|Moonabie Formation|34116|4|Described|p8|||Precambrian. See also pp9-10.||||||13-AUG-08
12217|Moonabie Formation|34269|6|Mentioned|Table 1|||||||||
12217|Moonabie Formation|34287|6|Mentioned|p35|||||||||
12217|Moonabie Formation|34319|6|Mentioned|p69|||||||||
12217|Moonabie Formation|34535|6|Mentioned|p52|||||||||
12217|Moonabie Formation|34537|5|Briefly described|p30|||||||||
12217|Moonabie Formation|35255|6|Mentioned|Fig.3|||||||||
12217|Moonabie Formation|35270|6|Mentioned|Fig.1|||||||||
12217|Moonabie Formation|35298|5|Briefly described|Table 1|||||||||
12217|Moonabie Formation|35706|6|Mentioned|Fig.1|||||||||
12217|Moonabie Formation|36003|6|Mentioned|Fig.8|||||||||
12217|Moonabie Formation|36073|6|Mentioned|p330|||||||||
12217|Moonabie Formation|36507|6|Mentioned|Fig.1|||||||||
12217|Moonabie Formation|36627|6|Mentioned|p82|||||||||
12217|Moonabie Formation|37461|6|Mentioned|p325|||||||||
12217|Moonabie Formation|37811|6|Mentioned|p222|||||||||
12217|Moonabie Formation|38068|5|Briefly described|p66|||||||||
12217|Moonabie Formation|39344|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
12217|Moonabie Formation|39349|6|Mentioned|Map legend|Mesoproterozoic|Paleoproterozoic|Early to Middle ProterozoicE - M||||||07-NOV-08
12217|Moonabie Formation|39352|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
12217|Moonabie Formation|39802|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
12217|Moonabie Formation|40445|6|Mentioned|p53|||||||||
12217|Moonabie Formation|40448|5|Briefly described|p36|||Formerly Moonabie Grit||||||
12217|Moonabie Formation|40644|6|Mentioned|p120 Fig. 2, p121|Paleoproterozoic|Paleoproterozoic|Massive volcanic grits which overlay the former "Moonabie Porphyry" and "Moonabie Volcanics" now referred to as McGregor Volcanics.||||||02-JUN-09
12217|Moonabie Formation|41402|6|Mentioned|p35|||||||||
12217|Moonabie Formation|41493|6|Mentioned|Table 1|||||||||
12217|Moonabie Formation|41609|6|Mentioned|Fig.1|||||||||
12217|Moonabie Formation|41667|5|Briefly described|p6|||||||||
12217|Moonabie Formation|41972|6|Mentioned|p366|||||||||
12217|Moonabie Formation|42469|6|Mentioned|p13|||Port Augusta, SI53-4||||||
12217|Moonabie Formation|42546|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
12217|Moonabie Formation|42736|5|Briefly described|map legend|Paleoproterozoic||||||||07-NOV-08
12217|Moonabie Formation|42934|5|Briefly described|p520 Fig.1|||Intruded by Charleston Granite.||||||12-JAN-10
12217|Moonabie Formation|43052|5|Briefly described|p66|||||||||
12217|Moonabie Formation|43053|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Volcaniclastic sandstone.||||||07-NOV-08
12217|Moonabie Formation|43141|6|Mentioned|p63,Fig.1|||||||||
12217|Moonabie Formation|43258|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
12217|Moonabie Formation|43298|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
12217|Moonabie Formation|44660|14|Not recorded|map legend||Carpentarian|Carpentarian, lithology.||||||
12217|Moonabie Formation|50605|5|Briefly described|p8.6|||Overlies and intertongues with: McGregor Volcanics. Geological Province: Gawler Craton and Curnamona Province.||||||13-AUG-08
12217|Moonabie Formation|60515|6|Mentioned|p116 Fig.1 |||||||||
12217|Moonabie Formation|60953|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Age: ~1740Ma. Volcaniclastic gritty sandstone and siltstone.||||||07-NOV-08
12217|Moonabie Formation|60954|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Geological Province: Gawler Craton.||||||07-NOV-08
12217|Moonabie Formation|61108|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|Volcaniclastic gritty sandstone and siltstone. Age: ~1740 Ma.||||||07-NOV-08
12217|Moonabie Formation|61307|5|Briefly described|p37|Paleoproterozoic|Paleoproterozoic|Geological Province: Gawler Craton.||||||07-NOV-08
12217|Moonabie Formation|61522|5|Briefly described|p5 Fig.1|||Geological Province: Gawler Craton.||||||
12217|Moonabie Formation|63020|5|Briefly described|p987 Fig. 8|Paleoproterozoic|Paleoproterozoic|Age: ~1750Ma. Geological Province: Gawler Craton (Spencer Domain).||||||07-NOV-08
12217|Moonabie Formation|63866|6|Mentioned|p9, p30|||||||||
12217|Moonabie Formation|64130|5|Briefly described| p1380 Fig.2, p1381 |||Eastern Gawler Craton.|1756 +/ -8 Ma (Jagodzinski, 2005).|||||
12217|Moonabie Formation|64722|6|Mentioned|Fig. 5 p.13|Paleoproterozoic|Paleoproterozoic|Of South Australian Craton.||||||
12217|Moonabie Formation|64739|6|Mentioned|p264 Fig.1. |Paleoproterozoic|Paleoproterozoic|Gawler Craton.||||||
12217|Moonabie Formation|64741|5|Briefly described|p299 Fig. 2|Paleoproterozoic|Paleoproterozoic|Age: 1770-1750Ma.||||||07-FEB-11
12217|Moonabie Formation|65221|5|Briefly described|p26|Palaeoproterozoic|Palaeoproterozoic|1745Ma, Cleve Domain. Intruded by Gawler Range Volcanics and Hiltaba Suite.||||||10-MAR-10
12217|Moonabie Formation|65375|6|Mentioned|p13, p19.|Paleoproterozoic|Paleoproterozoic|Northern Eyre Peninsula.|1740 Ma.|||||
12217|Moonabie Formation|65376|6|Mentioned|p8 Fig.1.1. |||||||||
12217|Moonabie Formation|65390|5|Briefly described|p23 Fig.3|Statherian|Statherian|Spencer Domain, Gawler Craton. Overlies McGregor Volcanics. Age of about 1740 - 1730 Ma inferred in Figure 3.||||||
12217|Moonabie Formation|65483|4|Described|p19, Fig 2|Palaeoproterozoic|Palaeoproterozoic|Overlies and intertongues with McGregor Volcanics at type locality in Moonabie Range. Intruded by the Cultana Subsuite. Poorly bedded volcaniclastic gritty sandstone to heavy mineral banded feldspathic quartzite.||||||27-JAN-11
12217|Moonabie Formation|65915|5|Briefly described|p5|Statherian|Statherian|Sedimentary and volcanic rocks deposited between ~1790-1740 Ma east of Kalinjala Mylonite Zone.||||||
12217|Moonabie Formation|65922|5|Briefly described|p13 Fig.4, p29 Fig. 6|Statherian|Statherian|Gawler Craton. Sedimentary formation. Age of ~1745-1670 Ma given.||||||
12217|Moonabie Formation|66302|5|Briefly described|p4 Fig.3, p28, p33, p46, p57, p63|Statherian|Statherian|Spencer Domain, Gawler Craton. Maximum depositional age, another age given is 1750 +/- 5 Ma (Fraser and Neumann, 2010) . A volcanic crystallisation age was also given at 1744 +/- 6 Ma (Fraser and Neumann, 2010)|1756 +/- 8 Ma (SHRIMP U-Pb, Jagodzinski, 2005)|||Interlayered with the McGregor Volcanics. Equivalent to the Wandearah Metasiltstone and Wallaroo Group. Unconformably overlain by the Corunna Conglomerate.|Volcaniclastic sedimentary rock with massive volcaniclastic grit and quartz sandstone.|
12217|Moonabie Formation|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Southern Gawler Craton.|1752 +/- 10 Ma.|||||
12217|Moonabie Formation|67536|6|Mentioned|Map Legend|Statherian|Statherian|Gawler Craton.|||||Volcaniclastic sandstone and siltstone.|
12217|Moonabie Formation|68158|5|Briefly described|p1-2, p4-6, p9-13, p15-17, p23-24|||The likely protoliths were the McGregor Volcanics. SHRIMP II maximum depositional age of 1756 +/- 8 Ma (Jagodzinski, 2005) ia also given. Sm-Nd values. Age and provenance discussed in detail.|1750+/-5 and 1755+/-5 Ma (max depositional ages).|||Is overlain unconformably by Backy Point Formation. Interbedded with McGregor Volcanics. Is intruded by Hiltaba Suite.|(Undifferentiated) metasandstone. Basal volcaniclastic metasandstone, conglomerate; quartzose metasiltstone, fine- to medium-grained feldspathic metasandstone. Abundant clasts of various acid volcanics.|
12217|Moonabie Formation|68208|6|Mentioned|p32 Fig.3|Paleoproterozoic|Paleoproterozoic|Grouped with McGregor Volcanics.||||||
12217|Moonabie Formation|69004|6|Mentioned|p18|||Gawler Craton.||||||
12217|Moonabie Formation|69048|6|Mentioned|p3|||Eyre Peninsula / Yorke Peninsula.|c.1775-1750 Ma.|||||
12217|Moonabie Formation|69649|6|Mentioned|p6 Fig.4|||||||||
12217|Moonabie Formation|69666|5|Briefly described|p25, p27-28, p31, p39|Paleoproterozoic|Paleoproterozoic|Source of some grey quartzite sediments in the Backy Point Formation.|c.1745 Ma.|||Is overlain unconformably by Beda Basalt.||
12217|Moonabie Formation|70027|5|Briefly described|p57,72|Statherian|Statherian|Geological province: Gawler Craton. Deposited at ca. 1750 Ma just prior to the 1730-1690 Ma Kimban Orogeny.  Coeval with Warramboo magnetite gneiss, Wallaroo Group, Price Metasediments.|ca. 1750 Ma|||||
12217|Moonabie Formation|70333|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Bedding rarely visible.|||||Massive grey to purplish volcaniclastic grit with pebble beds and heavy mineral laminae. Separately mapped: fine-medium feldspathic sandstone; arenaceous metasiltstone; medium to very coarse metasandstone; very coarse to pebbly lithic metasandstone.|
12217|Moonabie Formation|70334|4|Described|p2,8-11,14,17,39,41,43-44,67,74-75|Statherian|Statherian|Geological province: Gawler Craton. Type section: western Moonabie Range on WHYALLA. Originally described by Jack (1914) of a boulder bed at Hummock Hill. Deformed by Kararan Orogeny (1590-1555 Ma). Deposition commenced at ~1755 Ma, likely as a continuous shet from the Moonabie Range northwards. Detrital zircon geochronology studies consistently yield single age populations of ~1750 Ma, suggesting McGregor Volcanics as possibly the main detrital source however Hf isotopic studies show some inconsistency with that of the McGregor Volcanics, suggesting dilution/contamination by other clastic material. Intruded by Hiltaba Suite granites. Contemporaneous with Mcgregor Volcanics. Potentially deformed during Kararan Orogeny, with Corunna Conglomerate based in similarities in fold orientation and geometry. Affected by haematite-rich alternation, and contains minor tourmaline-quartz veining. See also p85-86,90.|c. 1755 Ma|||Overlain unconformably by Pandurra Formation or Beda Basalt or Backy Point Formation. Intruded by Gairdner Dolerite and Cultana Subsuite. Equivalent to Wallaroo Group.|Poorly bedded volcaniclastic gritty metasandstone; poorly sorted medium-coarse-grained lithic and arkosic sandstone; locally massive, feldspathic, containing heavy mineral bands, interbedded with lesser granule and pebble conglomerate and siltstone.|
12217|Moonabie Formation|70659|4|Described|p4, p9-11, p14, p29, p31, p36, p40, p44|Palaeoproterozoic|Palaeoproterozoic|See also p57-60, p62-106, p116, p275, p301, p303-319, p321-323, p342, p345, p381-389, p405-407. Part of basement to the Olympic Domain. Folded during Kararan Orogeny. Separated from Wandearah Formation by Angle Dam Fault. Major source of detritus for this unit was the McGregor Volcanics. Graphic core logs. Thin section descriptions.|~1750 Ma|||Intruded by Hiltaba Suite. Is overlain by Fresh Well Formation, Roopena Basalt, and the Wandearah Formation (thrust-faulted).|Massive, poorly sorted, fine- to coarse-grained arkosic and lithic sandstone containing rounded pebbles of quartzite, vein quartz, chert and felsic volcanics with rare cross bedding defined by heavy mineral laminations.|
12217|Moonabie Formation|70721|6|Mentioned|p64|Paleoproterozoic|Paleoproterozoic|||||||
12217|Moonabie Formation|70816|6|Mentioned|p3|Paleoproterozoic|Paleoproterozoic|Gawler Ranges region.||||||
12217|Moonabie Formation|70948|6|Mentioned|p974|Paleoproterozoic|Paleoproterozoic|Geological province: Gawler Craton.||||||
12217|Moonabie Formation|71037|5|Briefly described|p21, p22-23 Fig.2, p27 Fig.6, p21 Fig.1|Paleoproterozoic|Paleoproterozoic|U-Pb SHRIMP maximum depositional age 1755+/-5 Ma - 1750+/-5 Ma (Fraser and Neumann, 2010).|1755 +/- 5 Ma - 1750 +/- 5 Ma|||Shown as younger than Tip Top Granite and older than Wallaroo Group.|Grey to purplish massive to well-bedded sandstone, locally pebbly with heavy mineral laminae.|
12217|Moonabie Formation|71129|3|Fully described|p1,14,17-18,31-36,38,42-44,73,75,95-97|Statherian|Statherian|Geological Province: Olympic Domain, Gawler Craton. The type locality occurs in the Moonabie Range. Contains a dominantly c. 1755 Ma felsic volcanic source, interpreted to be from McGregor Volcanics. Occurs in outcrop in an extensive NNW-trending belt of discontinuous exposures extending southward to the Whyalla area, bounded to the east by Roopena Fault. Interpreted to have been deposited as lahar-like, sandy mass and hyperconcentrated flow deposits in a continental volcanic environment. Base of Moonabie Formation is undrilled, and therefore nature of basement to Moonabie Formation is unknown, but possibly include Mcgregor Volcanics or similar rocks to Corny Point Paragneiss or Donington Suite. Deformed, tilted and folded during c. 1610-1575 Ma Kararan Orogeny, prior to the overlying relatively-flat lying volcanosedimentary sequences, forming a hilly paleotopography, resulting in onlapping relationships with overlying stratigraphy. Intruded by Gluepot granite during Kimban Orogeny. Contains quartz-tourmaline veins and breccias associated with the Roopena Fault system. Juxtaposed against Pandurra Formation via Red Rock Fault, and Wandearah Formation via Angle Dam Fault. Intruded by Gluepot Granite, Angle Dam Volcanics and Gairdner Dolerite. Contact with the intrusive Gluepot Granite characterised by breccia zones of sandstone and quartzite clasts cemented by hydrothermal quartz and tourmaline. Lithology discussed in some detail.  Temporally equivalent to Wallaroo Group. See also p104-105,177,179-180, 182,184,187-188,199-201,203-206,225,227,230-231.|c. 1755 Ma (zircon)|||Unconformably overlain by Fresh Well Formation, Roopena Basalt, Pandurra Formation. Underlain by, and intertongues with Mcgregor Volcanics. Faulted against  the Broadview Schist.|Purple-brown, massive, poorly to moderately sortedm pebbly sandstones and weakly to well-bedded, moderately to well sorted, fine- to coarse-grained lithic sandstones and quartzites.|13-NOV-19
12217|Moonabie Formation|71130|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|SHRIMP U-Pb maximum depositional age by Fraser and Neumann (2010).|1755 +/- 5 Ma - 1750 +/- 5 Ma.||||Grey to purplish, massive to well-bedded sandstone, locally pebbly with heavy mineral laminae.|
12217|Moonabie Formation|71131|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|SHRIMP U-Pb maximum depositional age by Fraser and Neumann (2010).|1755 +/- 5 Ma - 1750 +/- 5 Ma.||||Grey to purplish, massive to well-bedded sandstone, locally pebbly with heavy mineral laminae.|
12217|Moonabie Formation|71235|5|Briefly described|p1, p5-p6, p8-p9|||Deformed and metamorphosed to upper greenschist-amphibolite grade during the Kimban Orogeny.|c. 1745 Ma|||Overlain by the Corunna Conglomerate.||
12217|Moonabie Formation|71236|4|Described|v, p5, p12, p17,|||Gawler Craton, Cultana Inlier. A type locality is located west of the Moonabie Range (~45km SW of Whyalla). Contact metamorphosed in the Cultana Inlier by the Cultana Subsuite. This unit has undergone haematite alteration. See also  p19-p21, p27, p29 fig 24.||||Intruded by the Cultana Subsuite. Overlies and intertongues with the McGregor Volcanics.|Poorly-bedded, volcaniclastic, gritty sandstone, elsewhere it is a massive heavy mineral-banded, feldspathic quartzite.|
12217|Moonabie Formation|71317|6|Mentioned|p15-p16|Palaeoproterozoic|Palaeoproterozoic|Olympic Domain, Gawler Craton.||||||
12217|Moonabie Formation|71341|6|Mentioned|p187 fig 6, p194, p196|||Broadly geochemically similar to the Myola Volcanics, McGregor Volcanics, Cleve Group, Price Metasediments and the Wallaroo Group.||||||
12217|Moonabie Formation|71348|6|Mentioned|p201|Statherian|Statherian|Geological province: Gawler Craton.||||||
12217|Moonabie Formation|71413|6|Mentioned|p32 Fig 2|||Geological province: Gawler Craton.||||||
12217|Moonabie Formation|71414|6|Mentioned|p42 Fig 1, p43|Statherian|Statherian|Geological province: Gawler Craton.|~1755 Ma.|||Intruded by Gluepot Granite.||
12217|Moonabie Formation|71534|6|Mentioned|p296|Statherian|Statherian|Geological province: Gawler Craton.||||||
12217|Moonabie Formation|71559|6|Mentioned|p15 Fig 1|Paleoproterozoic|Paleoproterozoic|Geological province: Gawler Craton.||||||
12217|Moonabie Formation|71859|5|Briefly described|p3-p4, p6|Paleoproterozoic|Paleoproterozoic|Olympic Domain, southern Gawler Craton.||||||
12217|Moonabie Formation|71862|6|Mentioned|p3, p9, p52-p53, p57|||||||Intruded by the Gluepot Granite (Moola Suite).||
12217|Moonabie Formation|72089|6|Mentioned|p3|Palaeoproterozoic|Palaeoproterozoic|Gawler Craton.||||||
12217|Moonabie Formation|72090|6|Mentioned|p10, p14|||Olympic Domain, Gawler Craton.||||||
12217|Moonabie Formation|72237|6|Mentioned|p29|Paleoproterozoic|Paleoproterozoic|Geological province: Gawler Craton.||||||
12217|Moonabie Formation|72462|5|Briefly described|p3, p10|Paleoproterozoic|Paleoproterozoic|Gawler Craton. In the Moonabie Range, it is dominated by coarse volcaniclastic detritus derived from the McGregor Volcanics, but at Hummock Hill and elsewhere in the North Whyalla Hills the sandstone is generally more mature.||||Equivalent to Wallaroo Group.|Medium- to coarse-grained generally massive arkosic and lithic sandstone to pebble conglomerate.|
12217|Moonabie Formation|72463|6|Mentioned|p2|Paleoproterozoic|Paleoproterozoic|||||||
12217|Moonabie Formation|73026|5|Briefly described|p6, p9|Paleoproterozoic|Paleoproterozoic|Eyre Peninsula/Yorke Peninsula.|c. 1750 Ma||||Grit, sandstone, conglomerate felsic and lesser mafic volcanics.|
12217|Moonabie Formation|73027|5|Briefly described|p6, p9|Palaeoproterozoic|Palaeoproterozoic|Eastern Eyre Peninsula/Yorke Peninsula.|c. 1750 Ma||||Grit, sandstone, conglomerate felsic and lesser mafic volcanics.|
12217|Moonabie Formation|73030|6|Mentioned|p2149|Statherian|Statherian|Gawler Craton.||||||
12217|Moonabie Formation|73103|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic||||||Massive grey to purplish volcaniclastic grit with pebble beds and heavy mineral laminae. Bedding rarely visible.|
12217|Moonabie Formation|73110|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|The five facies in the LITHOLOGY section are mapped separately.|||||Massive grey to purplish volcaniclastic grit with pebble beds and heavy mineral laminae. Volcaniclastic grit; very coarse/pebbly lithic metasandstone; medium-very coarse metasandstone; arenaceous metasiltstone; fine-medium feldspathic sandstone.|
12217|Moonabie Formation|73130|6|Mentioned|[poster] Fig.1|Paleoproterozoic|Paleoproterozoic|||||||28-OCT-22
12217|Moonabie Formation|73162|6|Mentioned|p448, p450-453|Paleoproterozoic|Paleoproterozoic|||||Onlapped unconformably by Gawler Range Volcanics. Underlies Angle Dam Dacite, Fresh Well Formation.|Includes sandstone, lithic sandstone with some hydrothermal brecciation and hematite-sericite-chlorite-dolomite alteration. Silicification, sericitisation and tourmaline breccias adjacent to contact with the Angle Dam Dacite.|
12217|Moonabie Formation|73234|6|Mentioned|p4, p19, p21|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. Associated with McGregor Volcanics.|c. 1750 Ma||||Includes volcaniclastic rocks.|
12217|Moonabie Formation|73235|6|Mentioned|p53|||Gawler Craton. Olympic region.||||||
12217|Moonabie Formation|73493|6|Mentioned|p716 Fig.3|||Gawler Craton.||||||
12217|Moonabie Formation|73525|5|Briefly described|p19 Fig.13|Statherian|Statherian|Spencer Domain.|1755+/-5 Ma crystallisation age||||Clastics.|
12225|Moonan Formation|22643|5|Briefly described|p191, fig3,6|Early Cambrian|Early Cambrian|||||||
12225|Moonan Formation|22766|5|Briefly described|Fig.2 p561|Middle Cambrian|Early Cambrian|||||||
12225|Moonan Formation|23981|5|Briefly described|p8-9 Fig. 4, p32|Toyonian|Toyonian|Conformably underlies Coobowie Limestone. Geol.Prov:Stansbury Basin. Arenaceous shale with calcareous laminae containing shelly fossils, acritarchs and bacterial filaments; coarsening beds of siltstone and.....Diiferent lithologies for var.parts of basin.||||||15-FEB-07
12225|Moonan Formation|24465|5|Briefly described|p345 Fig.2|Cambrian|Cambrian|Geological Province: Stansbury Basin.||||||19-JAN-05
12225|Moonan Formation|35255|6|Mentioned|Fig.8|||||||||
12225|Moonan Formation|36244|6|Mentioned|p2|||Refers Thomson et al.1976.||||||
12225|Moonan Formation|40856|6|Mentioned|Fig.23.6|||||||||
12225|Moonan Formation|42222|6|Mentioned|Table 1 P4|||||||||
12225|Moonan Formation|42225|4|Described|p225|||||||||
12225|Moonan Formation|44133|5|Briefly described|p4 Fig. 7.2, 17|Early Cambrian|Early Cambrian|Geological Province: Stansbury Basin.||||||
12225|Moonan Formation|60958|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Massive, bedded to laminated green-grey siltstone and fine-grained sandstone, occasionally with rip-up intraclasts. Geological Province: Stansbury Basin.||||||14-APR-05
12225|Moonan Formation|61121|5|Briefly described|Map legend|Early Cambrian|Early Cambrian|Massive bedded to laminated green-grey siltstone and fine-grained sandstone, occasionally with rip-up intraclasts. Geological Province: Stansbury Basin.||||||06-JUN-05
12225|Moonan Formation|62787|6|Mentioned|p82 Fig. 3|Cambrian|Cambrian|Geological Province: Stansbury Basin (SA).||||||07-FEB-11
12225|Moonan Formation|65375|4|Described|p27 Fig.5, p28 Fig.6. |Cambrian|Cambrian|No outcrops mapped on Yorke Peninsula. Filamentous and coccoidal microfossils suggest restricted marine to lagoonal environment. 61.7m thick in Port Julia 1A core.||||Overlies Stansbury Limestone. Is overlain by Coobowie Limestone.|Massive, bedded to laminated siltstone and fine-grained sandstone.|
12225|Moonan Formation|65892|5|Briefly described|p9 Fig.4. |Early Cambrian|Early Cambrian|Yorke Peninsula.||||Overlies Stansbury Formation. Is overlain by Coobowie Limestone. Correlative of Moodlatana Formation.||
12225|Moonan Formation|68735|6|Mentioned|p233 Fig.2, p235 Fig.3|Middle Cambrian|Early Cambrian|Stansbury Basin.||||||
12225|Moonan Formation|68993|6|Mentioned|p544 Fig.1|Early Cambrian|Early Cambrian|Yorke Peninsula.||||||
12287|Moorillah Siltstone Member|23287|6|Mentioned|Fig.3|||Age: Lower Ediacarian. of Sandison Subgroup.||||||
12287|Moorillah Siltstone Member|24195|5|Briefly described|p45 Fig.3|||Of the Brachina Formation. Overlain by Port Stanley Sandstone Member. Geological Province: Adelaide Geosyncline||||||
12287|Moorillah Siltstone Member|30807|6|Mentioned|p102|||Suggested map symbol||||||
12287|Moorillah Siltstone Member|34291|6|Mentioned|p19|||Adelaidean. See also PP75,76||||||
12287|Moorillah Siltstone Member|35586|6|Mentioned|p26|||Now to be known as Moorillah Formation.||||||
12287|Moorillah Siltstone Member|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Marinoan||||||
12287|Moorillah Siltstone Member|39808|6|Mentioned|p223|||||||||
12287|Moorillah Siltstone Member|41429|4|Described|p220|||||||||
12287|Moorillah Siltstone Member|42222|6|Mentioned|p18|||||||||
12287|Moorillah Siltstone Member|42600|5|Briefly described|p9|||Of Brachina Fmn.||||||30-SEP-08
12287|Moorillah Siltstone Member|43052|5|Briefly described|p192,table 6.1|||Of Brachina Formation.||||||30-SEP-08
12287|Moorillah Siltstone Member|60959|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Lamiated to massive, reddish coarse grained siltstone.||||||
12287|Moorillah Siltstone Member|61732|5|Briefly described|p28 Fig. 13|Marinoan|Marinoan|Of the Brachina Formation. Geological Province: Adelaide Rift Complex.||||||07-FEB-11
12287|Moorillah Siltstone Member|64455|5|Briefly described|p138 Fig. 1|Neoproterozoic III|Neoproterozoic III|Of Brachina Formation. Overlain by Bailey [Bayley?] Range Siltstone Member, underlain by Moolooloo Siltstone Member. Brown - mauve event beds, some tuffs brush marks of? Vendotaenids. Age is Edicaran.||||||12-MAY-16
12287|Moorillah Siltstone Member|67030|6|Mentioned|p409 Fig. 2|Ediacaran|Ediacaran|||Of Brachina Formation||Overlies the Moolooloo Siltstone Member, underlies the Bayley Range Siltstone Member.||26-APR-12
12287|Moorillah Siltstone Member|70406|5|Briefly described|p123, 121 Fig 5.|Neoproterozoic|Neoproterozoic|||Of Brachina Formation.||Overlies Moolooloo Siltstone Member. Lateral equivalent of Lincoln Gap Siltstone Member of Tent Hill Formation.||12-MAY-16
12287|Moorillah Siltstone Member|71129|5|Briefly described|p129|Ediacaran|Ediacaran|Of Adelaide Geosyncline.||Unit of Brachina Formation.||Correlable to Lincoln Gap Sandstone Member/Tent Hill Fm.||
12289|Moorlands Lignite Member|10010|5|Briefly described|p12 Fig. 3|Middle Eocene|Middle Eocene|Of the Olney Formation. Geological Province: Murray Basin.||||||13-AUG-07
12289|Moorlands Lignite Member|22773|5|Briefly described|Fig24.8p352|Middle Eocene|Middle Eocene|||||||
12289|Moorlands Lignite Member|22799|5|Briefly described|p24 Fig.10|Late Eocene|Late Eocene|||||||
12289|Moorlands Lignite Member|22857|5|Briefly described|p325 Fig.24.8|Middle Eocene|Middle Eocene|Of the Olney Formation. Geological Province: Murray Basin.||||||
12289|Moorlands Lignite Member|22887|5|Briefly described|Fig.6 p13|Late Eocene|Late Eocene|||||||
12289|Moorlands Lignite Member|22893|5|Briefly described|fig4 p9|Oligocene|Oligocene|||||||
12289|Moorlands Lignite Member|23671|6|Mentioned|p3|||Supersedes the Moorlands Coal Measures of Ludbrook (1961).  Of the Renmark Beds.||||||
12289|Moorlands Lignite Member|23818|5|Briefly described|p174 Fig.84, p179|Late Eocene|Late Eocene|Geological Province: Murray Basin. Of the Renmark Beds (Knight Group). Also referred to as "Moorlands Coal Measures".||||||21-JAN-05
12289|Moorlands Lignite Member|23884|5|Briefly described|p155 Fig. 13.2|Late Eocene|Late Eocene|Geological Province: Murray Basin.||||||
12289|Moorlands Lignite Member|30754|6|Mentioned|p13|||Distribution||||||
12289|Moorlands Lignite Member|30758|6|Mentioned|p166|||Middle-Upper Eocene age||||||
12289|Moorlands Lignite Member|31625|6|Mentioned|Fig. 5.2|||Eocene||||||
12289|Moorlands Lignite Member|34308|6|Mentioned|p179|||U.Eocene. Formerly "Moorlands C.M."||||||
12289|Moorlands Lignite Member|37132|5|Briefly described|p367|||||||||
12289|Moorlands Lignite Member|39329|6|Mentioned|Fig.1|||||||||
12289|Moorlands Lignite Member|42125|6|Mentioned|Fig.5 p132|||||||||01-NOV-22
12289|Moorlands Lignite Member|42130|6|Mentioned|Fig.3 p265|||||||||01-NOV-22
12289|Moorlands Lignite Member|42134|6|Mentioned|Fig.3 p335|||||||||01-NOV-22
12289|Moorlands Lignite Member|42137|6|Mentioned|Fig.2 p368|||||||||01-NOV-22
12289|Moorlands Lignite Member|42138|6|Mentioned|Fig.2 p390|||||||||01-NOV-22
12289|Moorlands Lignite Member|42717|6|Mentioned|map legend|Eocene|Paleocene|||||||
12289|Moorlands Lignite Member|42881|4|Described|Fig.3, P84|||||||||
12289|Moorlands Lignite Member|42966|2|Defined|Table 12|Late Eocene||of Olney Formation. Also of Renmark beds||||||
12289|Moorlands Lignite Member|43073|5|Briefly described|Table 3|||of Renmark Beds||||||
12289|Moorlands Lignite Member|43791|6|Mentioned|p372, Fig1|||||||||
12289|Moorlands Lignite Member|43804|6|Mentioned|Fig.2,p49|||||||||
12289|Moorlands Lignite Member|44133|5|Briefly described|p158|||Of the Olney Formation (Renmark Group). Geological Province: Murray Basin.||||||
12289|Moorlands Lignite Member|49038|5|Briefly described|p37|||||||||
12289|Moorlands Lignite Member|49040|6|Mentioned|Fig.6|||||||||
12289|Moorlands Lignite Member|61155|5|Briefly described|p18|Early Oligocene|Late Eocene|Of the Olney Formation. Geological Province: Murray Basin.||||||
12289|Moorlands Lignite Member|65552|6|Mentioned|p5 Fig. 3|Late Eocene|Late Eocene|Spelt Moorlands Lignite Mbr in figure. Western Murray Basin. Of Olney Formation.||||||
12289|Moorlands Lignite Member|72445|6|Mentioned|App.7 p7.|Late Eocene|Late Eocene|Shown on the 'Lithostratigraphy of Cenozoic sediments in the Murray Basin' as Moorlands Lignite Member (from Brown & Stephenson 1991). Shown as Moorland Lignite Member in the text.|||||Includes lignite.|
12289|Moorlands Lignite Member|73228|6|Mentioned|p54|||||Olney Formation, Renmark Group|||Lignite.|
12300|Moorowie Formation|941|4|Described|p917-920. |Early Cambrian|Early Cambrian|Of Mount (1970). Eastern Flinders Range. Deposited within a small complex extensional basin influenced by diapirism. Contains archaeocyaths, calcimicrobes, oncoid and laminar stromatolites, sphinctozoan sponges and coral-like skeletal fossils including a new, un-named tabulate cnidarian.|||||Interfingering siliclastic, dolostone and carbonate breccias, and quartzite conglomerate; coarse mixed siliclastic-carbonate and boundstones; channeled, coarse-grained arkosic and lithic sandstones interstratified with red siltstones and shales.|
12300|Moorowie Formation|23981|5|Briefly described|p8-9 Fig. 4, p53 Fig. 21|Early Cambrian|Early Cambrian|Comprises green-grey, rarely red, very calcareous sandstones, siltstones and mudstones; it contains intraformational conglomerates at many levels; interfingers with Oparinna Formation. Geol. Prov: Arrowie Basin. See also p55.||||||04-FEB-08
12300|Moorowie Formation|24176|4|Described|p16, p23 Tb. 1|Early Cambrian|Early Cambrian|Massive pale grey archaeocyathid and flaggy limestones, intertonguing with red-brown and green siltstones and green shales (with trilobites).  Max. thickness: 230m.  Geological Province: Mount Painter Province.||||||09-APR-08
12300|Moorowie Formation|30176|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
12300|Moorowie Formation|30801|6|Mentioned|p5|||Lower Cambrian. Table p5-6.||||||09-APR-08
12300|Moorowie Formation|30807|6|Mentioned|p102|||Suggested map symbol||||||
12300|Moorowie Formation|35255|6|Mentioned|Fig.8|||||||||
12300|Moorowie Formation|35395|6|Mentioned|p104|||Stratigraphy||||||
12300|Moorowie Formation|35835|6|Mentioned|p201|||||||||
12300|Moorowie Formation|36198|6|Mentioned|Fig.I.2|||||||||
12300|Moorowie Formation|40852|6|Mentioned|p33|||||||||
12300|Moorowie Formation|42011|6|Mentioned|p459|||||||||
12300|Moorowie Formation|42222|5|Briefly described|p20|||||||||
12300|Moorowie Formation|42225|6|Mentioned|Fig.4 P224|||||||||
12300|Moorowie Formation|42458|5|Briefly described|p698|||||||||
12300|Moorowie Formation|44133|5|Briefly described|p3, 25, 26, 4 Fig. 7.2, 12|Botomian|Botomian|Underlain by Mernmerna Formation. Geological Province: Arrowie Basin.||||||
12300|Moorowie Formation|60418|5|Briefly described|p135|Early Cambrian|Early Cambrian|Of the Hawker Group. Geological Province: Arrowie Basin of Adelaide Geosyncline.||||||18-MAY-05
12300|Moorowie Formation|60889|4|Described|p245 Fig.2, p248-9, p252-4|Early Cambrian|Early Cambrian|Prograding highstand reef complexes. Thickness: 230 m. Arrowie Basin. Shown as Moorowie Fm.||Hawker Group||Overlies Oraparinna Shale. Is overlain (unconformably?) by Coads Hill Member and Edeowie Limestone Member of Billy Creek Formation.|Consists of over 200 m of thick, fairly porous, vuggy limestone and archaeocyathan reef complexes.|21-SEP-17
12300|Moorowie Formation|60959|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of the Hawker Group. Prograding reef complexes of near-shore shale and siltstone, oolite and reef limestone.||||||
12300|Moorowie Formation|63447|4|Described|p961, 962-963, 964, 968, 979, Fig.2, 3|Early Cambrian|Early Cambrian|Shallow water sediments. Bioherm complexes form major part of unit. Four coral genera described.||Hawker Group||Laterally equivalent to the upper Wilkawillina Limestone, Mernmerna Formation (Parara Limestone), Oraparinna Shale.||
12300|Moorowie Formation|63569|6|Mentioned|p117 Fig.1|Early Cambrian|Early Cambrian|Arrowie Basin.||||||
12300|Moorowie Formation|65686|5|Briefly described|p406, p409 Fig 2|Early Cambrian|Early Cambrian|230m thick.||||Underlies the Coads Hill Member.||07-MAY-12
12300|Moorowie Formation|65892|5|Briefly described|p7 Fig.3, p9 Fig.4, p10. |Early Cambrian|Early Cambrian|Arrowie Basin. 230m thick. Contains prograding highstand reef complexes.||Unit in Hawker Group.||Is overlain by Billy Creek Formation.||
12300|Moorowie Formation|65925|5|Briefly described|p14 Fig.2.2, Appendix 2.|Early Cambrian|Early Cambrian||||||Shale, siltstone, shelf margin oolite, reef limestone.|
12300|Moorowie Formation|66518|6|Mentioned|p19 Fig.4.|Cambrian|Cambrian|Arrowie Basin.||Unit in Hawker Group.||Overlies Mernmerna Formation. Is overlain unconformably by Billy Creek Formation.||
12300|Moorowie Formation|68735|6|Mentioned|p234, p235 Fig.3|Early Cambrian|Early Cambrian|Arrowie Basin. Contains archaeocyathid-rich reef and biohermal complexes cut by erosional channels. Deposited during the worldwide Botoman transgression; contains some of the earliest known corals.||Hawker Group.||||10-APR-17
12300|Moorowie Formation|68993|6|Mentioned|p544 Fig.1|Early Cambrian|Early Cambrian|Arrowie Basin.||Of the Hawker Group.||||
12300|Moorowie Formation|71102|5|Briefly described|p242,250-251|||Of Arrowie Basin. Intersected section: NB (North Boundary Creek, Chambers Gorge, E Flinders Ranges). Archaeocyath-rich, oolitic sandy limestone (Fuller and Jenkins, 2007).|||||Interbedded limestone and sands, occasional slump folding.|
12300|Moorowie Formation|72429|3|Fully described|p949-952, p959, p965-973, p976-977|Lower Cambrian|Lower Cambrian|Mount Chambers Gorge, eastern Flinders Ranges. Facies indicates shallow marine regressive conditions and the development of a biologically diverse carbonate platform seaward of evaporitic lagoons and supratidal sabkhas. Megabreccias formed as thin semi-autochthonous debris aprons or shallow tidal-channel infills resulting from gradual and persistent wave rents. Shale interbeds represent lightly channelised shallow-marine ramp deposits with adjacent mud flats. Description and mapping provided originally by Mount (1970). Named after Moorowie Spring. Megabreccias are discussed in great detail, including clasts, clast sizes, shapes, formation and relevant depositional environments.||Hawker Group|Includes the Pinyatta Member, Wookata Shale Member, Kandramooka Member, Pack Creek Member and the Brillig Catch Member.|Overlies the Mernmerna Formation. Underlies the Billy Creek Formation. Equivalent in part to the Oraparinna Shale.|Massive archaeocyathan limestones, ooid grainstones, peloid limestones, reef-sourced megabreccias and red shales.|
12300|Moorowie Formation|73251|6|Mentioned|p36|Cambrian|Cambrian|Arrowie Basin, Moorowie and Yalkalpo Sub-basins. Thermally late to post-mature.||Hawker Group||Underlain by Mernmerna Formation. Unconformably overlain by Billy Creek Formation.||
12437|Mount Adams Quartzite|23394|5|Briefly described|Map legend|Proterozoic|Proterozoic|||||||
12437|Mount Adams Quartzite|23411|6|Mentioned|Map Legend|||||||||
12437|Mount Adams Quartzite|23818|6|Mentioned|p35|||Of the Brindana Schist.||||||
12437|Mount Adams Quartzite|24176|4|Described|p26 Tb. 1, p7|Proterozoic|Proterozoic|Of Radium Creek Metamorphics.  Feldspathic quartzite, minor phyllite.  Max. thickness: 210m.  Geological Province: Mount Painter Province.||||||
12437|Mount Adams Quartzite|30176|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
12437|Mount Adams Quartzite|30177|2|Defined|p123|Paleoproterozoic|Paleoproterozoic|See also p32.Prob.Lower Proterozoic. Type section: Two and a quarter miles southeast of Mount Adams, lat. 30degrees06'04"S, long. 139degrees32'45"E to lat. 30degrees06'48"S long. 139degrees32'50"E.||||||24-NOV-22
12437|Mount Adams Quartzite|30807|6|Mentioned|p103|||Suggested map symbol||||||
12437|Mount Adams Quartzite|30920|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Prob.Lower Proterozoic||||||07-NOV-08
12437|Mount Adams Quartzite|34537|6|Mentioned|p35|||||||||
12437|Mount Adams Quartzite|43052|5|Briefly described|p149|||||||||
12437|Mount Adams Quartzite|60953|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Feldspathic quartzite. Mount is Mt in text.||||||
12437|Mount Adams Quartzite|61108|5|Briefly described|map legend|Mesoproterozoic|Mesoproterozoic|Feldspathic quartzite. Mount is Mt in map legend.||||||11-SEP-07
12437|Mount Adams Quartzite|63489|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Included with undifferentiated quartzitic metasediments. Geological Province: Mount Painter Inlier.||||||10-SEP-07
12437|Mount Adams Quartzite|66302|6|Mentioned|p39, p49, p77|Mesoproterozoic|Mesoproterozoic|Moolawatana Domain, Curnamona Province.|1595 to 1591 Ma|||||
12437|Mount Adams Quartzite|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Mount Painter area.|1592 +/- 13 Ma.|||||
12437|Mount Adams Quartzite|67536|5|Briefly described|Map Legend|Calymmian|Calymmian|Curnamona Province. Written as Mt Adams Quartzite in text.|ca. 1576 +/- 2 Ma - 1575 +/- 14 Ma||||Quartzitic, pelitic and calcsilicate metasediments; volcanic rocks at Gunsight and Harts Creek.|
12437|Mount Adams Quartzite|67540|6|Mentioned|p33 Tb.3|||||Unit in Radium Creek Metamorphics.||Faulted against/intruded by Coulthard Suite.||04-FEB-16
12437|Mount Adams Quartzite|67653|6|Mentioned|p4|||Geological province: Curnamona Province.||||||
12437|Mount Adams Quartzite|69019|5|Briefly described|p18.|Calymmian|Calymmian|Age from detrital zircons.|c.1590-1580 Ma max. (Fanning et al 2003).|Of Radium Creek Metamorphics.||||
12437|Mount Adams Quartzite|69023|5|Briefly described|p14|||Detrital zircon maximum deposition age.|~1590-1580 Ma (Fanning et al., 2003).|||||
12437|Mount Adams Quartzite|69650|6|Mentioned|p8, p62, p64|||||Unit in Radium Creek Metamorphics.||Is intruded by Coulthard Suite.||
12437|Mount Adams Quartzite|69654|6|Mentioned|p3|||Curnamona Province.||||||
12437|Mount Adams Quartzite|70384|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Maximum U-Pb ICPMS age from detrital zircons.|<1590 +/- 8 Ma.|Radium Creek Group.|||Quartzite; minor schist. East of Paralana Fault Zone.|
12443|Mount Alexander Sandstone Member|23818|5|Briefly described|p141 Fig.65, p158|||Geological Province: Great Artesian Basin. Uppermost part of the Oodnadatta Formation. Max. thickness: 162 ft.||||||
12443|Mount Alexander Sandstone Member|24175|5|Briefly described|p28, p17 Fig. 3|Cenomanian|Albian|Of the Oodnadatta Formation.  Geological Province: Eromanga Basin.||||||
12443|Mount Alexander Sandstone Member|30804|6|Mentioned|Table 2|||||||||
12443|Mount Alexander Sandstone Member|30807|6|Mentioned|p102|||Suggested map symbol||||||
12443|Mount Alexander Sandstone Member|31249|6|Mentioned|p63|||||||||
12443|Mount Alexander Sandstone Member|33017|6|Mentioned|p5|||||||||
12443|Mount Alexander Sandstone Member|33075|6|Mentioned|Table 1|||Refers Wopfner et al. (1970)||||||
12443|Mount Alexander Sandstone Member|33491|4|Described|p56|||Mention Fig.2||||||
12443|Mount Alexander Sandstone Member|33825|6|Mentioned|p10|||Correlation table||||||
12443|Mount Alexander Sandstone Member|33828|6|Mentioned|Table 3|||||||||
12443|Mount Alexander Sandstone Member|33832|6|Mentioned|p11|||Stratigraphy & correlation||||||
12443|Mount Alexander Sandstone Member|33939|6|Mentioned|p386|||||||||
12443|Mount Alexander Sandstone Member|33971|6|Mentioned|Fig.29|||Strat. table.||||||
12443|Mount Alexander Sandstone Member|34611|6|Mentioned|p158|||Correlation chart. Fig.65||||||
12443|Mount Alexander Sandstone Member|36494|6|Mentioned|Fig.1|||||||||
12443|Mount Alexander Sandstone Member|36571|6|Mentioned|p101|||See also Table 4.||||||
12443|Mount Alexander Sandstone Member|38068|5|Briefly described|p72|||||||||
12443|Mount Alexander Sandstone Member|38814|6|Mentioned|Table 1|||||||||
12443|Mount Alexander Sandstone Member|39211|5|Briefly described|Fig.6|||See also Figs 9-12,14-16 etc. Correlation||||||
12443|Mount Alexander Sandstone Member|40801|6|Mentioned|p85|||||||||
12443|Mount Alexander Sandstone Member|40910|6|Mentioned|p16|||||||||
12443|Mount Alexander Sandstone Member|40911|6|Mentioned|Map legend|Cenomanian|Albian|Albian-?Cenomanian||||||
12443|Mount Alexander Sandstone Member|40925|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
12443|Mount Alexander Sandstone Member|40926|6|Mentioned|p17|||||||||
12443|Mount Alexander Sandstone Member|41064|6|Mentioned|p62|||||||||
12443|Mount Alexander Sandstone Member|41085|4|Described|p89|||||||||
12443|Mount Alexander Sandstone Member|41088|6|Mentioned|Fig.2|||||||||
12443|Mount Alexander Sandstone Member|41098|5|Briefly described|p177|||||||||
12443|Mount Alexander Sandstone Member|41266|6|Mentioned|Fig.3|||||||||
12443|Mount Alexander Sandstone Member|41523|5|Briefly described|p277|||||||||
12443|Mount Alexander Sandstone Member|42746|5|Briefly described|p12|||of Oodnadatta Formation (Freytag 1966). Now considered equivalent to Mackunda Formation.||||||
12443|Mount Alexander Sandstone Member|44133|5|Briefly described|p104 Fig. 9.11, 122|||Superseded in part by Mackunda Formation.||||||
12443|Mount Alexander Sandstone Member|44658|14|Not recorded|map legend|||Neoc-Albian. (G53-15).||||||
12443|Mount Alexander Sandstone Member|46937|6|Mentioned|Fig.10|||||||||
12443|Mount Alexander Sandstone Member|49010|6|Mentioned|Fig.4|||Eromanga Basin||||||
12443|Mount Alexander Sandstone Member|49011|6|Mentioned|Fig.3|||Eromanga Basin||||||
12443|Mount Alexander Sandstone Member|71321|6|Mentioned|p15|||Of Eromanga Basin.||||||
12453|Mount Alice Conglomerate|29658|6|Mentioned|p5|||||||||
12453|Mount Alice Conglomerate|36966|6|Mentioned|Table 1|||||||||
12453|Mount Alice Conglomerate|40926|3|Fully described|p34|||||||||
12453|Mount Alice Conglomerate|42905|5|Briefly described|p24, Fig 5.3|||actually spelt Mt Alice Conglomerate||||||
12461|Mount Anna Sandstone Member|12597|5|Briefly described|p492 Tb.1, p499|Barremian|Barremian|NW Eromanga Basin.||Unit in Cadna-owie Formation.|||Fluviatile, coarse-grained sandstone.|
12461|Mount Anna Sandstone Member|13516|6|Mentioned|p167 fig 10,  p171 fig 12|Early Cretaceous|Early Cretaceous|In Eromanga Basin.||Of Cadna-owie Formation||||
12461|Mount Anna Sandstone Member|23054|4|Described|p21,24||Aptian|||||||
12461|Mount Anna Sandstone Member|23818|5|Briefly described|p141 Fig.65, p152 Fig.72|Aptian|Aptian|Geological Province: Great Artesian Basin. Of the Cadna-owie Formation. Mount is spelt Mt. in text.||||||
12461|Mount Anna Sandstone Member|24175|5|Briefly described|p17 Fig. 3|Aptian|Barremian|Of Cadna-owie Formation.  Mount is Mt. in text of figure.  Geological Province: Eromanga Basin.||||||
12461|Mount Anna Sandstone Member|29379|6|Mentioned|Fig.11|||Refers Freytag 1966||||||
12461|Mount Anna Sandstone Member|30804|6|Mentioned|Table 2|||||||||
12461|Mount Anna Sandstone Member|30807|6|Mentioned|p102|||Suggested map symbol||||||
12461|Mount Anna Sandstone Member|31699|4|Described|p133|||L.Cretaceous||||||
12461|Mount Anna Sandstone Member|32314|6|Mentioned|Fig. 4|||||||||
12461|Mount Anna Sandstone Member|33075|6|Mentioned|p452|||Continuation of Wyandra Sst. Mb.?||||||
12461|Mount Anna Sandstone Member|33523|6|Mentioned|p17|||||||||
12461|Mount Anna Sandstone Member|33825|6|Mentioned|p10|||Correlation table||||||
12461|Mount Anna Sandstone Member|33828|6|Mentioned|p9|||||||||
12461|Mount Anna Sandstone Member|33939|2|Defined|p402|Aptian|Neocomian|Neocomian - Aptian||||||
12461|Mount Anna Sandstone Member|33971|6|Mentioned|Fig.29|||Strat. table.||||||
12461|Mount Anna Sandstone Member|33976|6|Mentioned|Fig.2|||||||||
12461|Mount Anna Sandstone Member|34611|5|Briefly described|p156|||See Fig.65||||||
12461|Mount Anna Sandstone Member|36214|6|Mentioned|p57|||||||||
12461|Mount Anna Sandstone Member|38068|4|Described|p72|||See also p71.||||||31-AUG-20
12461|Mount Anna Sandstone Member|38604|6|Mentioned|Map legend|Neocomian|Neocomian|||||||
12461|Mount Anna Sandstone Member|38605|4|Described|p20|||See also Table 4.||||||
12461|Mount Anna Sandstone Member|39211|5|Briefly described|Fig.6|||||||||
12461|Mount Anna Sandstone Member|40910|6|Mentioned|Table 3|||||||||
12461|Mount Anna Sandstone Member|40926|6|Mentioned|Table 2|||||||||
12461|Mount Anna Sandstone Member|41084|5|Briefly described|p81|||||||||
12461|Mount Anna Sandstone Member|41085|5|Briefly described|p88|||||||||
12461|Mount Anna Sandstone Member|41165|5|Briefly described|p360|||||||||
12461|Mount Anna Sandstone Member|41266|6|Mentioned|Fig.3|||||||||
12461|Mount Anna Sandstone Member|41523|5|Briefly described|p271|||||||||
12461|Mount Anna Sandstone Member|42283|5|Briefly described|p89|||||||||
12461|Mount Anna Sandstone Member|42465|5|Briefly described|Map Legend|||||||||
12461|Mount Anna Sandstone Member|42469|4|Described|p33|||||||||
12461|Mount Anna Sandstone Member|42520|6|Mentioned|p6|||Actually spelt Mt. Anna Sandstone Member.||||||
12461|Mount Anna Sandstone Member|42723|5|Briefly described|map legend|Neocomian||||||||
12461|Mount Anna Sandstone Member|42746|5|Briefly described|p11|||See also Fig.2||||||
12461|Mount Anna Sandstone Member|42816|6|Mentioned|p18|||of Cadna-owie Formation||||||
12461|Mount Anna Sandstone Member|43048|4|Described|Table 3.|||of Cadna-owie Formation||||||
12461|Mount Anna Sandstone Member|43071|6|Mentioned|p20|||of Cadna-owie Formation||||||
12461|Mount Anna Sandstone Member|43094|5|Briefly described|p43|||of Cadna-owie Formation||||||
12461|Mount Anna Sandstone Member|44133|5|Briefly described|p105 Fig. 9.12, 112|Cretaceous|Cretaceous|Geological Province: Eromanga Basin. Of the Cadna-owie Formation. Thickness: 40m.||||||
12461|Mount Anna Sandstone Member|44289|5|Briefly described|Map Legend||Aptian|||||||
12461|Mount Anna Sandstone Member|46791|5|Briefly described|p42|||||||||
12461|Mount Anna Sandstone Member|46937|6|Mentioned|Fig.10|||||||||
12461|Mount Anna Sandstone Member|49010|6|Mentioned|Fig.4|||Eromanga Basin||||||
12461|Mount Anna Sandstone Member|49011|6|Mentioned|Fig.3|||Eromanga Basin||||||
12461|Mount Anna Sandstone Member|65385|5|Briefly described|pS134 Fig.7|Early Cretaceous|Early Cretaceous|Of Cadna-owie Formation.||||||08-MAR-12
12461|Mount Anna Sandstone Member|69019|5|Briefly described|p85 Fig.21.|Aptian|Hauterivian|SW Eromanga Basin.||Unit in Cadna-owie Formation.||Is overlain by Bulldog Shale.||
12461|Mount Anna Sandstone Member|69023|6|Mentioned|p89 Fig.20|Aptian|Hauterivian|||||||
12461|Mount Anna Sandstone Member|69457|5|Briefly described|p41:3, 7|Early Cretaceous|Early Cretaceous|Wopfner et al. (1970). SW Eromanga Basin. Fluviatile-deltaic sediments.||Cadna-owie Formation.||||12-JUL-16
12461|Mount Anna Sandstone Member|69673|6|Mentioned|p154, p155 fig 127|Cretaceous|Cretaceous|||Cadna-owie Formation||Overlain by Bulldog Shale, Wallumbilla Formation||
12461|Mount Anna Sandstone Member|69946|4|Described|p19-20, p57, p95|Early Cretaceous|Early Cretaceous|Eromanga Basin. A thin bed occurs in the parent Formation's type section and thickens to the S, making up the entire Formation adjacent to the Gawler Ranges. Porphyry clasts are from the Gawler Range Volcanics, derived from the Gawler Craton. Deposited by N-flowing fluvial channels.||Unit in Cadna-owie Formation.|||Contains distinctive clasts of red volcanic porphyry.|
12461|Mount Anna Sandstone Member|70789|5|Briefly described|p318, p320 Fig.4|Early Cretaceous|Early Cretaceous|Eromanga Basin.|||||Well-sorted fluvial and deltaic sandstone beds.|
12461|Mount Anna Sandstone Member|70938|5|Briefly described|p807-p808|Early Cretaceous|Early Cretaceous|Abbreviated to Mt Anna Sandstone on p808.||Cadna-owie Formation.||||13-DEC-19
12461|Mount Anna Sandstone Member|71342|5|Briefly described|Ch5 p19-p20|Aptian|Barremian|Deposited by northeasterly flowing fluvial channels (Wopfner et al., 1970). Spore-pollen zone is given in Ch5 p57. See also  Ch5 p32, Ch5 p57, Ch5 p96.||Cadna-owie Formation|||Sandstone containing clasts of red volcanic porphyry.|
12461|Mount Anna Sandstone Member|73249|5|Briefly described|p319, p335|Aptian|Barremian|Eromanga Basin. Forms the top of the Cadna-owie Formation, restricted to the southwest of the basin. Contains pebbles derived from the Gawler Range Volcanics described by Wopfner et al., (1970), interpreted as a short-term glacial event.||Cadna-owie Formation||Underlies the Bulldog Shale.|Localised sandstone-rich layer with pebbles.|
12467|Mount Arrowsmith Volcanics|22671|3|Fully described|p838-39,841-42,847||Neoproterozoic III|These volcanics occur within the Kara beds. Previously mapped as part of Mount Wright Volcanics.  Max Age: 586 (+/-) 7 Ma. Mt Arrowsmith Volcanics in text.||||||17-JAN-06
12467|Mount Arrowsmith Volcanics|22772|5|Briefly described|p62,69,Table13.1|Neoproterozoic III|Neoproterozoic III|Max Age: 586 (+/-) 7 Ma.||||||
12467|Mount Arrowsmith Volcanics|22857|5|Briefly described|p62, Tb. 13.1 (insert p70-71)|Neoproterozoic III|Neoproterozoic III|Of the Kara beds. Age: 586+/-7Ma (U/Pb SHRIMP zircon). Geological Province: Kanmantoo Fold Belt. See also p402 App. 1 Tb.A1.3 and p94.||||||24-MAR-06
12467|Mount Arrowsmith Volcanics|22858|5|Briefly described|p94||Neoproterozoic|||||||
12467|Mount Arrowsmith Volcanics|23562|5|Briefly described|p295 Fig 2|Neoproterozoic III|Neoproterozoic III|Mount is Mt. in text.||||||
12467|Mount Arrowsmith Volcanics|23932|6|Mentioned|p667|||||||||
12467|Mount Arrowsmith Volcanics|24509|5|Briefly described|p42, p44 Tb. 2|Neoproterozoic|Neoproterozoic|Mount is Mt in text. Alkaline volcanics. Contains abundant pillow lavas, and breccias, hyaloclastites, volcanoclastic sediments, minor carbonate sediment; trachybasalt. Age: 586+/-7Ma (SHRIMP U-Pb zircon; Crawford et al 1997). Geol Prov: Koonenberry Belt.||||||04-MAY-05
12467|Mount Arrowsmith Volcanics|24551|6|Mentioned|p74|||||||||
12467|Mount Arrowsmith Volcanics|24599|5|Briefly described|p495 Fig. 2, p496|Neoproterozoic|Neoproterozoic|Transitional alkaline to tholeiitic basaltic metamorphosed lavas.  Age: 586+/-7Ma (Crawford et al, 1997).  Mount is Mt in text. Geological Province: Bancannia trough.||||||01-SEP-08
12467|Mount Arrowsmith Volcanics|36534|6|Mentioned|p226|||||||||
12467|Mount Arrowsmith Volcanics|42966|5|Briefly described|p299|||Proterozoic - Cambrian.||||||01-SEP-08
12467|Mount Arrowsmith Volcanics|43560|6|Mentioned|fig.1,p227|||||||||
12467|Mount Arrowsmith Volcanics|44093|5|Briefly described|p108, p110|Neoproterozoic|Neoproterozoic|Max Age: Late Neoproterozoic. Min Age: Late Neoproterozoic. Age: 586+/-7Ma (U/Pb SHRIMP zircon). Geological Province: Tasman Fold Belt.||||||18-MAR-05
12467|Mount Arrowsmith Volcanics|50129|6|Mentioned|p21 Fig.7|||Mount is Mt. in text.||||||
12467|Mount Arrowsmith Volcanics|50154|5|Briefly described|p59|Neoproterozoic|Neoproterozoic|Age: 586 +/- 7 Ma (Crawford et al., 1997).||||||
12467|Mount Arrowsmith Volcanics|60650|6|Mentioned|p189|||In NSW. Mount is Mt in text.||||||01-SEP-08
12467|Mount Arrowsmith Volcanics|62787|5|Briefly described|p75|||Of Crook (1980). Age: 586+/-7Ma (SHRIMP, Crawford et al. (1997)). Alkaline rocks.||||||07-FEB-11
12467|Mount Arrowsmith Volcanics|63489|5|Briefly described|Map legend|||Age: ?Neoproterozoic. Alkali basalt, trachybasalt, trachyte and related intrusives.||||||10-SEP-07
12467|Mount Arrowsmith Volcanics|63789|5|Briefly described|Map Legend|Early Cambrian|Proterozoic|Of Kara beds. Alkali basalt, trachybasalt, trachyte submarine and subaerial lava flows and sills, pyroclastics and related intrusives (gabbro, dolerite, diorite, syenite).||||||27-NOV-08
12467|Mount Arrowsmith Volcanics|63790|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Kara beds. Alkali basaltic, trachybasaltic, trachytic submarine and subaerial lava flows and sills, pyroclastics and related intrusives (gabbro, dolerite, diorite, syenite).||||||27-NOV-08
12467|Mount Arrowsmith Volcanics|63793|5|Briefly described|p19 Table 1, p30, 32.|||Separates the Kara beds into upper and lower parts.|586 +/- 7 Ma (Crawford et al. 1997).||||A transitional alkaline series of basaltic pillow lavas and pyroclastic tuffs; locally sub-aerial deposits; trachytic tuffs and lavas; melanocratic gabbro sills and small syenitic and dioritic intrusions.|19-JAN-15
12467|Mount Arrowsmith Volcanics|63848|5|Briefly described|p532, p538.|Ediacaran|Ediacaran|High-Nb suite, geochemically similar to volcanics from Red Creek, near Truro (SA).|586 +/- 7 Ma (SHRIMP zircon:Crawford et al. 1997).|||||
12467|Mount Arrowsmith Volcanics|64168|5|Briefly described|p31|Neoproterozoic|Neoproterozoic|Age: 586Ma. An alkali basaltic suite of rocks with associated intrusions.||||||14-MAY-08
12467|Mount Arrowsmith Volcanics|64671|5|Briefly described|Map legend|||Faulted into Kara beds. Intruded by a dacitic/rhyolitc dyke of the Cymbric Vale Formation. Rocks of the Gnalta Group are fault bounded against the Mount Arrowsmith Volcanics. Mount is Mt in text.||||||26-NOV-08
12467|Mount Arrowsmith Volcanics|64679|5|Briefly described|Map legend|Neoproterozoic III|Neoproterozoic III|Alkali basalt; trachybasalt, trachyte; rhyolite flows, sills; pyroclastic rocks.||||||27-NOV-08
12467|Mount Arrowsmith Volcanics|64680|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Kara beds? Part of Kara beds or faulted into Kara beds? Alkali basalt, trachybasalt, trachyte and related intrusives.||||||01-DEC-08
12467|Mount Arrowsmith Volcanics|64684|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Kara beds. Part of Kara beds or faulted into Kara beds? Alkali basalt, trachybasalt, trachyte and related intrusives.||||||
12467|Mount Arrowsmith Volcanics|64687|5|Briefly described|Map Legend|Early Cambrian|Proterozoic|Of Kara beds (part of Kara beds or faulted into Kara beds?). Oldest rocks in the Koonenberry region. Alkali basalt, trachybasalt, trachyte and related intrusives.||||||
12467|Mount Arrowsmith Volcanics|65381|5|Briefly described|p688, Fig. 2|Neoproterozoic|Neoproterozoic|Of the Wertago zone, Broken Hill; subalkaline volcanics. Part of the Kara beds.||||||26-MAR-13
12467|Mount Arrowsmith Volcanics|66623|1|Redefined|pp26-29, p v, p14. |Neoproterozoic|Neoproterozoic|Formerly part of Torrowangee Series (Mawson 1912), Wonominta Beds (Warris 1967), Kara beds (Mills 1992). First named Mount Arrowsmith Volcanics by Crook (1980). Separated from Mount Wright Volcanics (Crawford et al.1997) on basis of geochemistry.|585.5 +/- 3.2 Ma.|Unit in Grey Range Group.||Interfingers with sedimentary units (Kara Formation) of Grey Range Group.|Basalt-ferrobasalt-trachybasalt-trachyandesite-alkali rhyolite suite, subject to low grade regional metamorphism. Large, scoriaceous pillow lavas, pyroclastic rocks, sub-volcanic sills; rare subaerial flows and pyroclastic deposits; nundorite.|
12467|Mount Arrowsmith Volcanics|66917|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|||Unit in Grey Range Group.||Is overlain by Kara Formation.|Undifferentiated mafic igneous rocks; alkali basalt, trachybasalt, trachyte; submarine and subaerial lava flows, sills and related intrusions; regionally metamorphosed to greenschist facies.|
12467|Mount Arrowsmith Volcanics|66918|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Four un-named units are mapped separately.||Unit in Grey Range Group.|||Undifferentiated mafic igneous rocks; alkali basalt, trachybasalt, trachyte; submarine and subaerial lava flows, sills and related intrusions; regionally metamorphosed to greenschist facies.|
12467|Mount Arrowsmith Volcanics|66927|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Narrow trends of high magnetic intensity, continuous over many kilometres, parallel to sub-parallel and dislocated by fractures.||||Is overlain by Kara Formation.|Alkali basalt, trachybasalt, trachyte; submarine and subaerial flows, sills and related intrusions.|
12467|Mount Arrowsmith Volcanics|66929|5|Briefly described|Map legend|Early Cambrian|Late Proterozoic|||||Intruded by a Cymbric Vale Formation felsic dyke.|Alkali basalt, trachybasalt, trachyte and related intrusives; limestone and shale; nundorite; scoria horizons, pyroclastics, hyaloclastites and pillow breccias.|
12467|Mount Arrowsmith Volcanics|66933|5|Briefly described|Map legend|Early Cambrian|Late Proterozoic|Includes, or is faulted into, Kara beds.|||||Alkali basalt, trachybasalt, trachyte and related intrusives; volcanic sediments including scoria horizons, pyroclastics, hyaloclastites and pillow breccias; trachytic tuffs, locally subaerial with accretionary lapilli and compaction welding.|
12467|Mount Arrowsmith Volcanics|67105|5|Briefly described|p651, 653-655, 659, 661, 663, 666|Ediacaran|Ediacaran|Crawford et al. (1997) distinguished these rocks from the Mount Wright Volcanics. Wonnaminta Zone, Koonenberry Belt. Clearly related to intra-plate rifting. Shares close geochemical affinities with the Farnell Group.|585.5 +/- 2.6 Ma (SHRIMP II U-Pb: Black, 2007).|Grey Range Group.||Equivalent to the Farnell Group.|Intercalated alkaline dominantly basaltic submarine lavas and related intrusives; rift-related. Rare rhyodacite.|
12467|Mount Arrowsmith Volcanics|67207|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|||Unit in Grey Range Group.|||Undifferentiated mafic igneous rocks; alkali basalt, trachybasalt, trachyte; submarine and subaerial lava flows, sills and related intrusions; regionally metamorphosed to greenschist facies.|
12467|Mount Arrowsmith Volcanics|67208|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Eleven un-named sub-units with differing lithologies are mapped separately.||Upper unit in Grey Range Group.|||Mafic igneous rocks: alkali basalt, trachybasalt, trachyte; submarine and subaerial lava flows, sills and related intrusions; gabbro plugs; mafic pyroclastics, hyaloclastites and pillow breccias; pillow basalt; microgabbro.|
12467|Mount Arrowsmith Volcanics|68241|5|Briefly described|p21, p24 Fig.3, p32, p33 Fig.3|Ediacaran|Ediacaran|Spelt as Mt Arrowsmith Volcanics in the text. > 4000 m thick.|586+/-7Ma SHRIMP U-Pb zircon Crawford et al. 1997|||Intertongued by the Sturts Meadows Siltstone.||
12467|Mount Arrowsmith Volcanics|69841|5|Briefly described|p19|Ediacaran|Ediacaran|Western NSW. Possible correlate of mid-Ediacaran mafic volcanic rocks of Tasmania.|c.586 Ma.|||||
12467|Mount Arrowsmith 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.||||||
12467|Mount Arrowsmith Volcanics|69961|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|No outcrop in map area.||Unit in Grey Range Group.|||Undifferentiated mafic igneous rocks: alkali basalt, trachybasalt, trachyte; submarine and subaerial lava flows, sills and related intrusions; regionally metamorphosed to greenschist facies.|
12467|Mount Arrowsmith Volcanics|70125|6|Mentioned|p400||||586 Ma (crystallisation age).|||||
12467|Mount Arrowsmith Volcanics|70648|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|9 un-named units: Microperthitic intrusion, commonly altered. Foliated albite-aegirine-nepheline-natrolite rock (nundorite); an altered alkaline tuff or intrusion. Undifferentiated mafic intrusions. Plugs and plutons of mafic (alkaline) gabbro, hornfelsed contacts and some alteration. Plagioclase-pyroxene plug or dyke, commonly altered. Mafic volcaniclastic rocks including pyroclastics, hyaloclastites, pillow breccias. Trachyte including trachytic tuffs. Latite or trachy-basalt with large skeletal feldspar phenocrysts. Coarse-grained, serpentinite-chlorite ultramafic rock,originally picrite.||Grey Range Group|Includes 9 un-named units.||Undifferentiated mafic igneous rocks; alkali basalt, trachybasalt, trachyte; submarine and subaerial lava flows, sills and related intrusions; regionally metamorphosed to greenschist facies.|
12467|Mount Arrowsmith Volcanics|70650|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|4 unnamed units: Plugs and plutons of mafic (alkaline) gabbro, hornfelsed contacts, some internal metamorphic epidote-albite-chlorite-quartz alteration. Fine- to medium-grained plagioclase-pyroxene plug or dyke, commonly altered. Mafic volcaniclastic rocks including pyroclastics (eg. scoria beds), hyaloclastites and pillow breccias. Grey, feldspar-rich trachyte including trachytic tuffs, some subaerial with compaction welding and accretionary lapilli.||Grey Range Group|Includes 4 un-named units.||Mafic igneous rocks; alkali basalt, trachybasalt, trachyte; submarine and subaerial lava flows, sills and related intrusions; regionally metamorphosed to greenschist facies.|
12467|Mount Arrowsmith Volcanics|70744|6|Mentioned|p940|||Has an alkaline intraplate character considered characteristic of modern rifts.||||||
12467|Mount Arrowsmith Volcanics|70749|5|Briefly described|p43|Neoproterozoic|Neoproterozoic|Southern Thomson and Koonenberry area.|~596 Ma.|||||
12467|Mount Arrowsmith Volcanics|70838|5|Briefly described|p268-270, p274, p278, p281|Ediacaran|Ediacaran|Coeval with Kara Formation. Geochemistry suggests a continental rift setting during emplacement.|585 +/- 3.2 Ma (Black, 2007).|Grey Range Group.|||Mafic rocks.|
12467|Mount Arrowsmith Volcanics|71262|5|Briefly described|p3-4, p5 Fig 2, p8 Fig 5, p9, p12|Neoproterozoic|Neoproterozoic||||||Alkali basalts with minor ultramafic rocks|
12467|Mount Arrowsmith Volcanics|71415|5|Briefly described|p10,15|||Geological province: SW Thomson Orogen. Of the Kooneberry Belt; of Eromanga Basin.||Unit of Grey Range Group.||Overlain by the Teltawongee Group and Ponto Group.||19-AUG-19
12467|Mount Arrowsmith Volcanics|71593|5|Briefly described|p121-p122, p188-p189|||Koonenberry Belt. Associated with Ni-Cu prospects.|c. 586 Ma||||Ultramafic volcanics.|
12467|Mount Arrowsmith Volcanics|71966|6|Mentioned|p989|Ediacaran|Ediacaran|Geological province: Delamerian Orogen. Of the Koonenbery Belt.|c. 586 Ma|||Correlable to Bathampton Metamorphics.||
12467|Mount Arrowsmith Volcanics|73059|6|Mentioned|p1061|||||||||
12467|Mount Arrowsmith Volcanics|73177|5|Briefly described|p1098, 1114-1115 Figs.16-17|Neoproterozoic|Neoproterozoic|Delamerian Orogen.||Grey Range Group.|||Alkaline volcanics.|
12467|Mount Arrowsmith Volcanics|74367|5|Briefly described|p18-19|Ediacaran|Ediacaran|Koonenberry Belt. Tentatively correlated to the Aruhna Subgroup.|585.5+/-3.2 Ma SHRIMP U-Pb zircon||||Silicic igneous formation, includes rhyolite.|
12481|Mount Barker Quartzite|23818|6|Mentioned|p103|||Of the Strangway Hill Formation (although previously assigned to Hawker Group).||||||
12481|Mount Barker Quartzite|30801|6|Mentioned|p5|||Strangway Hill Formation. Table P5-6.||||||
12481|Mount Barker Quartzite|32791|5|Briefly described|p13|||See also P11||||||
12481|Mount Barker Quartzite|33471|6|Mentioned|p556|||||||||
12481|Mount Barker Quartzite|34612|5|Briefly described|p103|||Probably member Strangway Hill Formation||||||
12481|Mount Barker Quartzite|35039|6|Mentioned|p365|||||||||
12481|Mount Barker Quartzite|39843|6|Mentioned|p58|||||||||
12481|Mount Barker Quartzite|40503|4|Described|p108|||||||||
12481|Mount Barker Quartzite|42243|5|Briefly described|p211|||||||||
12481|Mount Barker Quartzite|42505|5|Briefly described|Map legend|Adelaidean (Marinoan)||Superseded(?) by ABC Range Quartzite.||||||
12481|Mount Barker Quartzite|43759|6|Mentioned|p450|||||||||
12565|Mount Caernarvon Greywacke Member|22510|5|Briefly described|table1p37|||Age: Sturtian. Central Flinders Ranges||||||
12565|Mount Caernarvon Greywacke Member|30801|6|Mentioned|p5|||Tapley Hill Formation. Table P5-6||||||
12565|Mount Caernarvon Greywacke Member|30802|6|Mentioned|p12|||Sturtian. See also P14||||||
12565|Mount Caernarvon Greywacke Member|30807|6|Mentioned|p103|||Suggested map symbol||||||
12565|Mount Caernarvon Greywacke Member|32510|6|Mentioned|Fig.1|||||||||
12565|Mount Caernarvon Greywacke Member|34267|6|Mentioned|p105|||||||||
12565|Mount Caernarvon Greywacke Member|39344|6|Mentioned|Map legend|Precambrian|Precambrian|Sturtian to MarinoanSturtian||||||
12565|Mount Caernarvon Greywacke Member|40294|6|Mentioned|p49|||||||||
12565|Mount Caernarvon Greywacke Member|41405|3|Fully described|p165|||||||||
12565|Mount Caernarvon Greywacke Member|42882|4|Described|p9, Table 1 p3|||of Tapley Hill Formation||||||
12565|Mount Caernarvon Greywacke Member|43052|5|Briefly described|p189,Table 6.1|||of Tapley Hill Formation||||||
12565|Mount Caernarvon Greywacke Member|60959|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Of the Tapley Hill Formation. Fine grained green lithic sandstone. Diamictite interbeds.||||||
12565|Mount Caernarvon Greywacke Member|64846|6|Mentioned|p208 Fig.11 |Cryogenian|Cryogenian|Appears in a restricted space in Fig.11 as Mt Caernarvo Greywacke.||||||
12565|Mount Caernarvon Greywacke Member|65925|5|Briefly described|Appendix 2.||||||||Greywacke, with lenticular diamictite.|
12565|Mount Caernarvon Greywacke Member|67979|4|Described|p537-8, p529, p531 Fig.2, p542-3, p545|Sturtian||Name used interchangeably with Mount Caernarvon Greywacke (appears to be a casual shortening) in this article. Shown as Member in Fig 8 and in discussion. Presented as Mt Caernarvon Greywacke Member. In Alpana section this unit non-conformably overlies the Blinman salt diapir.||Tapley Hill Formation.|||Interbedded calcareous siltstones, fine to medium-grained sandstones, suggestive of turbidite environment|22-SEP-14
12565|Mount Caernarvon Greywacke Member|70407|5|Briefly described|p103 Fig 2|Neoproterozoic|Neoproterozoic|Age: Sturtian.||Of Tapley Hill Formation.|Includes Cox Sandstone Member.|||
12576|Mount Chandler Sandstone|22746|5|Briefly described|Fig.3 p515|Ordovician|Ordovician|Spelt Mt Chandler Sandstone||||||
12576|Mount Chandler Sandstone|22922|6|Mentioned|34|||||||||
12576|Mount Chandler Sandstone|23054|6|Mentioned|p36|||||||||25-MAR-21
12576|Mount Chandler Sandstone|23282|2|Defined|p80||Late Ordovician|Equiv to Pacoota Sandstone of Amadeus Basin. 'Mount Chandler Sandstone' introduced by Coats (1963), redefined by Benbow (1982). DO NOT CONFUSE WITH CHANDLER FORMATION OF AMADEUS BASIN. of Munda Group, Officer Basin. Age: Late Ordovician 457-450Ma.||||||06-SEP-06
12576|Mount Chandler Sandstone|23288|6|Mentioned|Fig.5||Early Ordovician|||||||
12576|Mount Chandler Sandstone|23524|5|Briefly described|p221 Fig. 3|Ordovician|Ordovician|Mount is Mt. in text.||||||
12576|Mount Chandler Sandstone|23818|5|Briefly described|p108|Ordovician|Ordovician|Presence of Scolithus and Cruziana fossils.||||||
12576|Mount Chandler Sandstone|23858|5|Briefly described|p917|Ordovician|Cambrian|Geological Province: Officer Basin.||||||
12576|Mount Chandler Sandstone|24067|5|Briefly described|p242|Paleozoic|Paleozoic|Geological Province: Officer Basin.||||||07-NOV-08
12576|Mount Chandler Sandstone|24112|5|Briefly described|p254  Fig.2|Late Ordovician|Early Ordovician|Mount is spelt Mt. in text. Of the Munda Group. Geological Province: Officer Basin||||||
12576|Mount Chandler Sandstone|30075|6|Mentioned|p12|||||||||
12576|Mount Chandler Sandstone|30544|6|Mentioned|p49|||||||||
12576|Mount Chandler Sandstone|30807|6|Mentioned|p102|||Suggested map symbol||||||
12576|Mount Chandler Sandstone|30923|6|Mentioned|Map legend|Mesozoic|Paleozoic|Palaeozoic - Mesozoic||||||07-NOV-08
12576|Mount Chandler Sandstone|31457|6|Mentioned|p13|||||||||
12576|Mount Chandler Sandstone|31698|6|Mentioned|Map legend|Middle Ordovician|Early Ordovician|?Lower to ?Middle Ordovician||||||
12576|Mount Chandler Sandstone|31969|6|Mentioned|p9|||||||||
12576|Mount Chandler Sandstone|31972|6|Mentioned|p4|||Cambro-Ord. age relationships||||||
12576|Mount Chandler Sandstone|32431|5|Briefly described|p99|||||||||
12576|Mount Chandler Sandstone|33491|6|Mentioned|p55|||||||||
12576|Mount Chandler Sandstone|33523|6|Mentioned|p20|||||||||
12576|Mount Chandler Sandstone|33578|6|Mentioned|p77|||Ordovician||||||
12576|Mount Chandler Sandstone|33738|6|Mentioned|p58|||||||||
12576|Mount Chandler Sandstone|34280|6|Mentioned|p10|||L.Ord.||||||
12576|Mount Chandler Sandstone|34610|6|Mentioned|p178|||Ordovician||||||
12576|Mount Chandler Sandstone|34612|3|Fully described|p111|||Ordovician. P108. Fossils P111.||||||
12576|Mount Chandler Sandstone|35149|6|Mentioned|Table 4|||||||||
12576|Mount Chandler Sandstone|35628|4|Described|Table 3|||||||||
12576|Mount Chandler Sandstone|36096|6|Mentioned|Fig.3|||||||||
12576|Mount Chandler Sandstone|36128|6|Mentioned|p13|||||||||
12576|Mount Chandler Sandstone|36491|6|Mentioned|Fig.2|||||||||
12576|Mount Chandler Sandstone|36920|6|Mentioned|Table 1|||||||||
12576|Mount Chandler Sandstone|38022|6|Mentioned|Fig.4|||||||||
12576|Mount Chandler Sandstone|38329|1|Redefined|p208|Ordovician|Ordovician|See also P194.||||||
12576|Mount Chandler Sandstone|39352|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
12576|Mount Chandler Sandstone|40003|5|Briefly described|Table 15|||||||||
12576|Mount Chandler Sandstone|40136|5|Briefly described|p32|||||||||
12576|Mount Chandler Sandstone|40926|6|Mentioned|p11|||||||||
12576|Mount Chandler Sandstone|40945|6|Mentioned|Fig.3|||||||||
12576|Mount Chandler Sandstone|43052|5|Briefly described|p198|||||||||
12576|Mount Chandler Sandstone|43053|5|Briefly described|Map Legend|Devonian|Ordovician|Spelt Mt Chandler Sandstone. Of the "Munda Sequence". Shallow marine to deltaic sandstone, siltstone and shale.||||||25-MAY-05
12576|Mount Chandler Sandstone|43258|5|Briefly described|Map Legend|Devonian|Ordovician|||||||
12576|Mount Chandler Sandstone|43298|5|Briefly described|Map Legend|Devonian|Ordovician|||||||
12576|Mount Chandler Sandstone|43657|6|Mentioned|Fig.3,p4||Ordovician|||||||
12576|Mount Chandler Sandstone|43690|6|Mentioned|Fig.2,p157||Cambrian|||||||
12576|Mount Chandler Sandstone|43732|6|Mentioned|Fig.4,p5||Early Ordovician|||||||
12576|Mount Chandler Sandstone|43743|6|Mentioned|Fig.2,p33||Ordovician|||||||
12576|Mount Chandler Sandstone|44109|5|Briefly described|p22 Fig. 22|Ordovician|Ordovician|Geological Province: central Officer Basin. Mount is Mt in text of figure.||||||
12576|Mount Chandler Sandstone|44133|4|Described|p40, 4 Fig. 7.2|Middle Paleozoic|Early Paleozoic|Geological Province: Eastern Officer Basin. Of the 'Munda Sequence'. Gradationally overlies Byilkaoora Formation. Disconformably overlies: Trainor Hill Sandstone, Marla Group. Correlated with Boongar beds.||||||07-NOV-08
12576|Mount Chandler Sandstone|44535|4|Described|map legend||Ordovician|(G/53-9).||||||
12576|Mount Chandler Sandstone|45149|6|Mentioned|p43|||See also Table 1.||||||
12576|Mount Chandler Sandstone|49792|5|Briefly described|Fig.5|||||||||
12576|Mount Chandler Sandstone|60953|5|Briefly described|Map Legend|Silurian|Silurian|Of the Munda Group. Mount is Mt in text.||||||27-APR-05
12576|Mount Chandler Sandstone|61108|5|Briefly described|map legend|Silurian|Silurian|Spelt Mt on map legend. Of Munda Group. Shallow marine to fluviodeltaic sandstone, siltstone and shale. Age: ?Silurian.||||||02-JUN-05
12576|Mount Chandler Sandstone|62570|5|Briefly described|p580 Figs. 2 and 3|Middle Cambrian|Middle Cambrian|Geological Province: Officer Basin. Mount is Mt in text.||||||10-AUG-07
12576|Mount Chandler Sandstone|65313|5|Briefly described|p578, p580 Fig. 8|Early Ordovician|Late Cambrian|Officer Basin. Ungoolya 1 well.||Of Munda Group.||Overlies Table Hill and Kulyong Volcanics (484 +/- 4 Ma and 483.6 +/- 20 Ma K-Ar dates); underlies Indulkana Shale.||26-MAR-12
12576|Mount Chandler Sandstone|69445|5|Briefly described|p30:5-6, 17|||Officer Basin.||||Overlies Kulyong Formation (now Table Hill Volcanics).||12-JUL-16
12576|Mount Chandler Sandstone|71146|5|Briefly described|p6|Late Ordovician|Middle Ordovician|Officer Basin.||Munda Group||Unconformably overlies the Table Hill Volcanics. Overlain by the Indulkana Shale and Blue Hills Sandstone.|Sandstone.|
12576|Mount Chandler Sandstone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone|
12576|Mount Chandler Sandstone|72478|5|Briefly described|p8|Late Ordovician|Early Ordovician|Officer Basin.|c. 495 Ma-450 Ma|Munda Group|Includes the Byilkaoora Member.|Overlies the Kulyong Formation. Underlies the Indulkana Shale.||25-MAR-21
12576|Mount Chandler Sandstone|73090|5|Briefly described|p12 Fig.7, Appendix|Silurian|Ordovician|||Munda Group.|||Sandstone, well-rounded, fine- to medium-grained quartz; sandstone, feldspathic, burrowed.|
12576|Mount Chandler Sandstone|73099|5|Briefly described|Map legend.|Ordovician|Ordovician|Officer Basin.||Munda Group.|||Pale grey and white to orange-brown (weathered), kaolinitic, very fine to coarse quartz sandstone with thin interbeds of white to dark red-brown claystone and siltstone.|
12576|Mount Chandler Sandstone|73109|5|Briefly described|Map legend.|Devonian|Ordovician|Subcrop and minor outcrop.|||||Orange-brown, very fine- to fine-grained quartz sandstone, bioturbated in part.|
12583|Mount Christie Metajaspilite|34904|6|Mentioned|p143|||||||||
12583|Mount Christie Metajaspilite|41609|6|Mentioned|p126|||||||||
12583|Mount Christie Metajaspilite|61556|5|Briefly described|p9-10 Figure|Paleoproterozoic|Paleoproterozoic|In Mount Christie area - central province. Mount is Mt in text of figure.||||||20-FEB-17
12596|Mount Cornish Formation|9694|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Geological Province: Georgina Basin. Underlies: Oorabra Arkose. Blue-grey diamictite.||||||
12596|Mount Cornish Formation|33102|6|Mentioned|Fig.2|||||||||
12596|Mount Cornish Formation|33699|6|Mentioned|p445|||||||||
12596|Mount Cornish Formation|35005|5|Briefly described|p145|||||||||
12596|Mount Cornish Formation|36473|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
12596|Mount Cornish Formation|36898|6|Mentioned|p181|||||||||
12596|Mount Cornish Formation|37572|5|Briefly described|p154|||||||||
12596|Mount Cornish Formation|37929|4|Described|p525|||||||||
12596|Mount Cornish Formation|38157|6|Mentioned|Table IX|||||||||
12596|Mount Cornish Formation|39210|4|Described|p51|||||||||
12596|Mount Cornish Formation|40538|5|Briefly described|Map legend|Adelaidean|Adelaidean|Tillite; siltstone; varvite. Geological Province: Georgina Basin.||||||15-NOV-05
12596|Mount Cornish Formation|40906|4|Described|p18|||||||||
12596|Mount Cornish Formation|41005|6|Mentioned|Fig.2|||||||||
12596|Mount Cornish Formation|41405|6|Mentioned|p205|||||||||
12596|Mount Cornish Formation|42059|6|Mentioned|Fig.2 P131|||||||||
12596|Mount Cornish Formation|42504|5|Briefly described|p72|||In the Georgina Basin.||||||08-NOV-06
12596|Mount Cornish Formation|42643|6|Mentioned|Fig.4 P19|||||||||
12596|Mount Cornish Formation|44158|6|Mentioned|p29|||In the Georgina Basin.||||||08-NOV-06
12596|Mount Cornish Formation|44233|14|Not recorded|Fig.1||Adelaidean|||||||
12596|Mount Cornish Formation|44327|2|Defined|Tb.I,p.7,8,13,14,18||Neoproterozoic|(F53-11). U.Prot. may be correlated with Areyonga Formation. Map.||||||08-NOV-06
12596|Mount Cornish Formation|44328|14|Not recorded|map legend||Neoproterozoic|Upper Proterozoic.||||||
12596|Mount Cornish Formation|45041|6|Mentioned|p45|||Correlates with Olympic Member||||||
12596|Mount Cornish Formation|45052|2|Defined|p67|Adelaidean|Adelaidean|||||||
12596|Mount Cornish Formation|45155|6|Mentioned|Fig.7|||In theGeorgina Basin.||||||08-NOV-06
12596|Mount Cornish Formation|46865|6|Mentioned|p49|||||||||
12596|Mount Cornish Formation|48844|2|Defined|p.1,16-20,22-3|||F.26,57,58,67,Pl.8. (new name). Overlain by Elyuah orFormation. Glacial origin. (F53-11).||||||08-NOV-06
12596|Mount Cornish Formation|48990|1|Redefined|p13|Adelaidean|Adelaidean|||||||
12596|Mount Cornish Formation|60122|6|Mentioned|p9|||||||||
12596|Mount Cornish Formation|60551|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Underlies Oorabra Arkose; overlies Yackah beds. Geological province: Georgina Basin.  Diamictite, siltstone, varved beds.||||||08-NOV-06
12596|Mount Cornish Formation|61404|5|Briefly described|Map legend|Cryogenian|Cryogenian|Of the Aroota Group. Tillite, siltstone, varvite. Geological Province: southern Georgina Basin.||||||
12596|Mount Cornish Formation|63562|6|Mentioned|p338 fig 3, p352 fig 10|Cryogenian|Cryogenian|Of Georgina Basin.||||Correlated with Areyonga Formation.||
12596|Mount Cornish Formation|64068|3|Fully described|p45, p223, p viii|Cryogenian||Correlated with Yardida Tilite.||Of Aroota Group.||Disconformably overlies Yackah beds; is disconformably overlain by Oorabra Arkose.|Several hundred metres of blue-green diamictite with interbeds of varvite and siltstone; minor sandstone, arkose and dolostone.|04-APR-12
12596|Mount Cornish Formation|64103|6|Mentioned|p404|||Geological Province: Georgina Basin.||||||07-FEB-11
12596|Mount Cornish Formation|64778|6|Mentioned|p13|Neoproterozoic|Neoproterozoic|Dulcie Syncline, Southern Georgina Basin.||||||
12596|Mount Cornish Formation|68270|4|Described|p680-683,686-688|Cryogenian|Cryogenian|Southern Georgina Basin. Type section occurs 4km WSW to 4.8km SSW of Mount Cornish; lat. 22'49'S, long. 136'27'E. Less than 365m thick. Glacial and periglacial deposit. Correlative to Sturt Tillite. Lateral equivalent to Yardida Tillite. Related to Sturt glaciation.||||Overlain disconformably by Oorabra Arkose. Underlain disconformably by Yackah beds.|Poorly bedded blue-green diamictite with interbeds of green varve-like siltstone, minor sandstone, arkose and dolostone; possible lower marker cap dolomite.|03-JUL-19
12596|Mount Cornish Formation|69437|5|Briefly described|p22:4-5, 7|Cryogenian|Cryogenian|SE Georgina Basin, Centralian A Superbasin. Supersequence 2.||Aroota Group.|||Glacial sedimentary rocks.|12-JUL-16
12596|Mount Cornish Formation|69439|6|Mentioned|p24:7|||Georgina Basin.||||Correlated with Naburula Formation (Ngalia Basin).||12-JUL-16
12596|Mount Cornish Formation|69443|4|Described|p28:6-8, 32-33|Cryogenian|Cryogenian|K.G. Smith (1964). Mount Cornish, Georgina Basin. Unfossiliferous. Small discontinuous outcrops. Generally 12-34m thick; 680m in the type section. Glacial and periglacial deposits. Part of the hangingwall of the Ooomoolmilla and Lucy Creek Faults; interpreted as rift basin fill in half grabens.||Aroota Group.||Disconformably overlies Yackah beds. Is overlain disconformably by Oorabra Arkose. Correlated with Yardida Tillite.|Diamictite with interbeds of varvite and siltstone; minor sandstone, arkose and dolostone. Some diamictite clasts are faceted and striated.|12-JUL-16
12596|Mount Cornish Formation|69673|4|Described|p114 fig 92|Cryogenian|Cryogenian|Maximum thickness of 680m.||Aroota Group|||Diamictite with interbeds of varvite and siltstone; minor sandstone and dolostone.|
12596|Mount Cornish Formation|72515|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Jervois Range Special Map Sheet. Georgina Basin.||Aroota Group|||Diamictite, interbedded varvite, siltstone; minor sandstone, arkose and dolostone.|
12596|Mount Cornish Formation|72516|3|Fully described|p13, p72, p79, p85-87|Cryogenian|Cryogenian|Georgina Basin. Type section occurs 4km west-southwest of Mount Cornish in southeast JERVOIS RANGE SPECIAL; also exposed in the Elua Range in Jinka. Deposited in a glacial to periglacial environment. Maximum thickness of 680m in the type section, however structural repitition is interpreted; 12-34m thick in Jinka. Equivalent to the Yardida Tillite and Central Mount Stuart Formation. See also p96-97, p154, p186, p195, p218.||Aroota Group||Unconformably overlies the Boundary Igneous Complex. Disconformably overlies the Yackah beds. Disconformably overlain by the Oorabra Arkose.|Poorly sorted, medium to very thickly bedded, blue green diamictite interbedded with laminated varvite and siltstone, minor sandstone, arkose and dolostone layers.|
12596|Mount Cornish Formation|73086|6|Mentioned|p62, p158|||Georgina Basin.||||Correlates to Areyonga Formation.||
12599|Mount Crawford Granite Gneiss|31292|6|Mentioned|p6|||Refers Mills (1963)||||||
12599|Mount Crawford Granite Gneiss|32457|4|Described|p100|||||||||
12599|Mount Crawford Granite Gneiss|44133|5|Briefly described|p56 Table 7.3|||Highly foliated granitic gneiss.||||||
12599|Mount Crawford Granite Gneiss|64647|3|Fully described|p38, p38 Fig. 1, p39, p39 Fig. 2, p40|Neoproterozoic|Neoproterozoic|Age: 812+/-6Ma (Pb/Pb). Relict granitic, though strongly foliated, texture and lack of compositional layering idicates intrusive origin.||||||
12599|Mount Crawford Granite Gneiss|73188|6|Mentioned|p315, p352|Tonian|Tonian|Interpreted to have intruded into an east-dipping mid-crustal extensional shear zone during the earliest Adelaidean phase of continental rifting.|812 +/- 6 Ma||||Deformed, within-plate A-type granite.|14-NOV-22
12599|Mount Crawford Granite Gneiss|73262|6|Mentioned|p580|Tonian|Tonian||812 +/- 6 Ma|||Intrudes Barossa Complex.||
12599|Mount Crawford Granite Gneiss|74367|5|Briefly described|p12, p18, p20|Tonian|Tonian|Age is of the precursor granite.|812+/-6 Ma SHRIMP igneous zircon|||Unconformably underlies Aldgate Sandstone, Burra Group||
12609|Mount Currie Conglomerate|22566|5|Briefly described|p73|Early Cambrian|Neoproterozoic|Of the Pertaoorrta Group.||||||08-NOV-06
12609|Mount Currie Conglomerate|22650|4|Described|p 160|||Age - Cambrian p 159.||||||
12609|Mount Currie Conglomerate|22651|5|Briefly described|p 173|||Precise age uncertain,  suggested approx. age of 600-580 Ma.||||||08-NOV-06
12609|Mount Currie Conglomerate|22763|6|Mentioned|p400|||||||||
12609|Mount Currie Conglomerate|22804|5|Briefly described|p444||Neoproterozoic|Of the Pertaoorrta Group.||||||08-NOV-06
12609|Mount Currie Conglomerate|22826|6|Mentioned|p568|Cambrian|Neoproterozoic|||||||
12609|Mount Currie Conglomerate|24301|3|Fully described|p17, p7 Tb. 2|Cambrian|Neoproterozoic|Defined by Forman (1955). Is divided into three informal units. Maximum thickness: 6100m. Unconformably overlies Winnall Sandstone. Geological Province: Amadeus Basin||||||24-SEP-08
12609|Mount Currie Conglomerate|24302|5|Briefly described|Map Legend|Cambrian|Cambrian|Geological Province: Amadeus Basin||||||
12609|Mount Currie Conglomerate|24496|5|Briefly described|p21 Tb.2|Cambrian|Cambrian|Geological Province: Amadeus Basin.||||||
12609|Mount Currie Conglomerate|24497|5|Briefly described|Map legend|Early Paleocene|Neoproterozoic|Geological Province: Amadeus Basin.||||||
12609|Mount Currie Conglomerate|24499|5|Briefly described|Map legend|||Mount is Mt. in text.  Geological Province: Amadeus Basin.||||||
12609|Mount Currie Conglomerate|30815|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
12609|Mount Currie Conglomerate|30817|4|Described|p9|||See also p14.||||||08-NOV-06
12609|Mount Currie Conglomerate|33307|6|Mentioned|Fig.6|||||||||
12609|Mount Currie Conglomerate|33478|6|Mentioned|Table 1|||||||||
12609|Mount Currie Conglomerate|33568|6|Mentioned|p45|||||||||
12609|Mount Currie Conglomerate|35102|6|Mentioned|Fig.2|||||||||
12609|Mount Currie Conglomerate|35308|6|Mentioned|p454|||||||||
12609|Mount Currie Conglomerate|36473|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
12609|Mount Currie Conglomerate|38157|6|Mentioned|Table VI|||||||||
12609|Mount Currie Conglomerate|39213|6|Mentioned|Fig.6|||Amadeus Basin Succession||||||
12609|Mount Currie Conglomerate|39565|6|Mentioned|p32|||||||||
12609|Mount Currie Conglomerate|40740|6|Mentioned|p1|||||||||
12609|Mount Currie Conglomerate|40910|6|Mentioned|p13|||||||||
12609|Mount Currie Conglomerate|41115|6|Mentioned|p1389|||||||||
12609|Mount Currie Conglomerate|41723|6|Mentioned|Map legend|Neoproterozoic|Early Cambrian|||||||
12609|Mount Currie Conglomerate|41852|6|Mentioned|Table 1|||||||||
12609|Mount Currie Conglomerate|41884|4|Described|p70|||||||||
12609|Mount Currie Conglomerate|42018|6|Mentioned|p540|||||||||
12609|Mount Currie Conglomerate|42504|5|Briefly described|p76|||||||||
12609|Mount Currie Conglomerate|42940|5|Briefly described|Plate 2|Cambrian|Cambrian|Conglomerate, arkose.  Age: 590-500Ma. Geological province: Amadeus Basin.||||||23-JAN-08
12609|Mount Currie Conglomerate|43035|4|Described|p20|||||||||
12609|Mount Currie Conglomerate|43503|6|Mentioned|50|Early Cambrian|Proterozoic|||||||
12609|Mount Currie Conglomerate|43756|6|Mentioned|p542|||||||||
12609|Mount Currie Conglomerate|43869|4|Described|p9, p10, p12|||Age: >550 Ma.  Geological Province: Amadeus Basin.||||||12-SEP-05
12609|Mount Currie Conglomerate|44109|5|Briefly described|p164|Cambrian|Cambrian|Thick, poorly sorted conglomerate and boulder lenses, with clasts up 1m across. Geological Province: Amadeus Basin.||||||
12609|Mount Currie Conglomerate|44439|14|Not recorded|p.7||Precambrian|Probably equivalent to Ellis Sandstone & Sir Frederick Conglomerate. Tentatively uppermost Precambrian. (G52-1).||||||
12609|Mount Currie Conglomerate|44493|4|Described|p.11, map|||BLOODS RANGE sheet. (G53-3). See p.8,10,12, for details.||||||08-NOV-06
12609|Mount Currie Conglomerate|44494|14|Not recorded|map legend||Cambrian|||||||
12609|Mount Currie Conglomerate|44495|4|Described|p.6, map||Cambrian|AYERS ROCK sheet (G52-8). See p.8,10 for details.||||||08-NOV-06
12609|Mount Currie Conglomerate|44496|5|Briefly described|map legend||Cambrian|Conglomerate; arkose at Ayers Rock possible lithological variant.||||||02-DEC-04
12609|Mount Currie Conglomerate|44505|14|Not recorded|p.3,7,8, Fig.1, Tb.1||Cambrian|||||||
12609|Mount Currie Conglomerate|44506|14|Not recorded|map legend||Proterozoic|||||||
12609|Mount Currie Conglomerate|45041|4|Described|p46|||L.Cambrian||||||
12609|Mount Currie Conglomerate|45170|5|Briefly described|p7|||||||||
12609|Mount Currie Conglomerate|48863|2|Defined|p.14|||Tb.1. opp. p.7,15. (G52-4) ?Cambrian.||||||
12609|Mount Currie Conglomerate|48864|2|Defined|p.29|||Tb.1. On many pages. p.1,9,10,24,27,38,31,42,47,Pl.11,13. (G52-3,7,8). ?Cambrian.||||||
12609|Mount Currie Conglomerate|48865|14|Not recorded|Fig.4.opp.p.10|||(G52-4).||||||
12609|Mount Currie Conglomerate|48963|6|Mentioned|Fig.3|||||||||
12609|Mount Currie Conglomerate|50286|5|Briefly described|Map Legend|Cambrian|Cambrian|Geological Province: Amadeus Basin.||||||22-DEC-09
12609|Mount Currie Conglomerate|60572|5|Briefly described|Map legend|Cambrian|Cambrian|Geological Province: Amadeus Basin.||||||23-DEC-09
12609|Mount Currie Conglomerate|60660|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Non-magnetic molasse basin sediments.||||||22-FEB-05
12609|Mount Currie Conglomerate|60662|5|Briefly described|Map Legend|||Molasse basin sediments.||||||22-FEB-05
12609|Mount Currie Conglomerate|60678|5|Briefly described|Map legend|Cambrian|Cambrian|Conglomerate containing clasts of sandstone, quartzite, felsic and mafic volcanics, granite, gneiss, mafic intrusives.  Geological Province: Amadeus Basin.||||||11-JAN-05
12609|Mount Currie Conglomerate|60679|5|Briefly described|Map Legend|Cambrian|Cambrian|Conglomerate with clasts of volcanics, granite and basalt. Geological Province: Amadeus Basin.||||||
12609|Mount Currie Conglomerate|60683|4|Described|p25-26, p9 Tb. 1|Cambrian|Cambrian|Includes the Ampiara member.  Unconformably overlies the Winnall beds. Geological Province: Musgrave Block/Amadeus Basin.||||||20-APR-05
12609|Mount Currie Conglomerate|61154|5|Briefly described|p26, p29|||Molasse deposits in the Mulga Park Domain, containing metamorphic epidote and locally actinolite. Age: 1062+/-6Ma (for contained rhyolite clast from Musgrave Block: Kober Pb-Pb age).  Geological Province: Musgrave Block.||||||19-JUL-05
12609|Mount Currie Conglomerate|61306|5|Briefly described|p11, p24|Cambrian|Cambrian|At Kata Tjuta and Mount Currie - in the Kata Tjuta complex. Geological Province: Amadeus Basin. See also p30, p46 Fig. 12 and p78-82 Appendix figures.||||||
12609|Mount Currie Conglomerate|61386|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Contains the Ampiara member. Coarse conglomerate, with rounded clasts of fine-grained porphyritic and banded rhyolite and less abundant rhyodacite, granite, amygdaloidal basalt in an epidotised arkosic matrix. Geological Province: Amadeus Basin.||||||23-DEC-09
12609|Mount Currie Conglomerate|61732|6|Mentioned|p96|||Overlie Winnall beds.||||||07-FEB-11
12609|Mount Currie Conglomerate|62376|5|Briefly described|p18|Early Cambrian|Late Proterozoic|Of the Pertaoorrta Group. Geological Province: Amadeus Basin.||||||09-FEB-10
12609|Mount Currie Conglomerate|62379|5|Briefly described|p7 Fig. 2|Early Cambrian|Late Proterozoic|Of the Pertaoorrta Group. Geological Province: Amadeus Basin.||||||
12609|Mount Currie Conglomerate|62609|5|Briefly described|Map Legend|Cambrian|Proterozoic|Conglomerate, arkose at  Ayers Rock.||||||08-NOV-06
12609|Mount Currie Conglomerate|62620|5|Briefly described|Map Legend|Cambrian|Proterozoic|Conglomerate, arkose at Ayers Rock.||||||
12609|Mount Currie Conglomerate|64068|6|Mentioned|p224|||Amadeus Basin. Correlated with Shadow Group, Georgina Basin.||||||
12609|Mount Currie Conglomerate|64103|6|Mentioned|p401|Early Cambrian|Ediacaran|Geological Province: Amadeus Basin.||||||07-FEB-11
12609|Mount Currie Conglomerate|64809|5|Briefly described|p2, p3 Fig.2 |Early Cambrian|Late Proterozoic|Deposited in Mount Currie Sub-basin during Petermann Orogeny.||Unit in Pertaoorrta Group.||||
12609|Mount Currie Conglomerate|65194|5|Briefly described|p64 Fig.4.9|Cambrian|Cambrian|Bedrock outcrops around Uluru.||||||11-APR-16
12609|Mount Currie Conglomerate|65233|5|Briefly described|p3 Fig. 2, p7|Early Cambrian|Neoproterozoic|Of the Pertaoorrta Group. Geological province: Amadeus Basin. Coarse. Clastic rocks in SW of basin which probably interfinger with Arumbera Sandstone.||||||07-FEB-11
12609|Mount Currie Conglomerate|65256|4|Described|piii, p6 Tb.1, p11, p16, p19|Cambrian||Molasse-type sediments from Petermann Orogeny uplift. Up to 6-7 km thick. Pb-Pb Kober zircon date for a rhyolite clast 1062+/-6 Ma; likely sourced from Tjauwata Group.||||Unconformably overlies Pinyinna beds, Winnall beds; correlated with Arumbera Sandstone.|Well-rounded clasts of quartzite; lower section is oligomictic comprising sandstone clasts; becomes polymictic and dominated by porphyritic rhyolite clasts up-section; upper part grades into dominantly granitic clasts.|19-MAY-14
12609|Mount Currie Conglomerate|67128|5|Briefly described|p13, p29|||Appears as Mount Currie conglomerate on p13. Kober Pb evaporation age from a rhyolite clast.|<1062 +/- 6 Ma (Young et al., 2002).|||||
12609|Mount Currie Conglomerate|67326|5|Briefly described|p2, p4|Early Cambrian|Neoproterozoic|Amadeus Basin.||Pertaoorrta Group.||Overlies Eninta Formation. Is overlain by Cleland Sandstone and tempe Formation.||
12609|Mount Currie Conglomerate|67856|6|Mentioned|p338 fig 4-30|Early Cambrian|Neoproterozoic|||Of Pertaoorta Group.||||
12609|Mount Currie Conglomerate|68100|6|Mentioned|p27|||Amadeus Basin. Detrital zircon ages mentioned.||||||
12609|Mount Currie Conglomerate|68270|5|Briefly described|p683|Ediacaran|Ediacaran|Amadeus Basin.||||Underlain by Sir Fred Conglomerate and Ellis Sandstone.||
12609|Mount Currie Conglomerate|68323|6|Mentioned|p4 Fig.2|Early Cambrian|Neoproterozoic|Amadeus Basin.||Pertaoorrta Group.||||
12609|Mount Currie Conglomerate|68733|6|Mentioned|p189 Fig.8|Ediacaran|Ediacaran|Mount spelt as Mt in text. Shown as underlying (sic) the Winnall Beds.||||||05-DEC-17
12609|Mount Currie Conglomerate|69436|5|Briefly described|p21:4, 20|Paleozoic|Paleozoic|Mount Currie Sub-basin, Amadeus Basin. Coarse fluvial sediments deposited in a flexural downwarping produced by the Petermann Orogeny.||||||12-JUL-16
12609|Mount Currie Conglomerate|69437|5|Briefly described|p22:10|Cambrian|Cambrian|Idirriki Sub-basin, SW Amadeus Basin.||||Is overlain by Maurice Formation.||12-JUL-16
12609|Mount Currie Conglomerate|69438|4|Described|p23:2-4, 20-23, 26-27, 44|Early Cambrian|Ediacaran|Forman (1963). Amadeus Basin. Estimated thickness is 6100m; 650m is exposed at Mount Olga (Kata Tjuta). Previously correlated with the Arumbera Sandstone. Probably late syntectonic to post-tectonic with the later phases of the 580-530 Ma Petermann Orogeny. Metamorphosed to greenschist facies. Lithologies are described in some detail.||Pertaoorrta Group.||Unconformably overlies Winnall beds. Is correlated with the Mutitjulu Arkose.|A thick succession of coarse pebble, cobble and boulder conglomerate.|12-JUL-16
12609|Mount Currie Conglomerate|69443|6|Mentioned|p28:14|||Amadeus Basin.||||Correlated with (part of) the Shadow Group.||12-JUL-16
12609|Mount Currie Conglomerate|69673|6|Mentioned|p64 fig 53, p65|||||||||
12609|Mount Currie Conglomerate|70018|5|Briefly described|p234-235|Neoproterozoic|Neoproterozoic|Amadeus Basin. Of Supersequence 4 in the southern Amadeus Basin. Equivalent to Ayers Rock Arkose. Correlable to Arumbera Sandstone in the northern Amadeus Basin.||||Underlain by Winnall Beds.||
12609|Mount Currie Conglomerate|70839|4|Described|p324,329-330,341-345|Cambrian|Cambrian|Of the southern Amadeus Basin. Part of Supersequence 4. Estimated thickness: 6km (as base of unit is not exposed). Interpreted to represent local remnants of proximal foreland deposition from Petermann Orogeny (Forman, 1966; Wells et al., 1970; Lindsay and Korsch, 1991). Detrital zircon analysis suggest a Musgrave region source (Pitjantjatjara Supersuite; Camacho et al., 2002) and additional minor Warakurna Supersuite component. Metamorphosed to greenschist-facies (Edgoose et al., 2004) indicating significant burial. Juxtaposed in outcrop against Winnall Beds unit 4 at one locality on the AYERS ROCK 1:250,000 geological map sheet near Yulara (Forman, 1965; Young et al., 2002). Alternative possibility from this study suggests this unit dates from late in the development of c. 1.0 Ga Ngaanyatjarra Rift.||||Underlain unconformably by Winnall beds. Equivalent to Mutitjulu Arkose.|Thick boulder conglomerate. Clasts include fresh igneous and metamorphic rocks including granite, basalt, and other lithologies.|
12609|Mount Currie Conglomerate|71088|5|Briefly described|p1, p8-p10, p12, p25-p27|Cambrian|Cambrian|Amadeus Basin. Assigned by previous authors to Supersequence 4, a lack of zircons younger than c. 1 Ga warrants a reassessment of their stratigraphic and structural relationships (according to the authors). Potentially unconformably overlies the Winnall beds.||||Equivalent (assumed) to the Mutitjulu Arkose.||
12609|Mount Currie Conglomerate|71114|5|Briefly described|p170 fig 1b|Terreneuvian|Ediacaran|SW Amadeus Basin.||||Shown as lateral equivalent to Ellis Sandstone, Sir Frederick Conglomerate.||14-FEB-18
12609|Mount Currie Conglomerate|71170|5|Briefly described|p91, p95|||Metamorphic evidence suggests this unit was deeply buried.||||||
12609|Mount Currie Conglomerate|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||quartzite, sandstone|
12609|Mount Currie Conglomerate|71279|5|Briefly described|p355 Fig.2|Early Cambrian|Ediacaran|Amadeus Basin.||Pertaoorrta Group.||||
12609|Mount Currie Conglomerate|71592|5|Briefly described|Appendix A.|||Musgrave Province. Contains a rhyolite clast dated at 1062 +/- 6 Ma.|||||Includes clast of rhyolite.|
12609|Mount Currie Conglomerate|71800|5|Briefly described|p26-p27|Early Cambrian|Early Cambrian|Amadeus Basin.||||Overlies the Maurice Formation. Unconformably overlain by the Chandler Limestone.|Sandstone.|
12609|Mount Currie Conglomerate|71841|5|Briefly described|p1|Early Cambrian|Ediacaran|Of Amadeus Basin.||Unit of Pertaoorrta Group.||Surrounded by Winnall beds. Also grades into Ellis Sandstone.||
12609|Mount Currie Conglomerate|71842|5|Briefly described|p3|Early Cambrian|Ediacaran|Of Amadeus Basin.||Unit of Pertaoorrta Group.||Correlable to Ellis Sandstone, Sir Frederick Conglomerate and Winnall Beds.||
12609|Mount Currie Conglomerate|72358|6|Mentioned|p118|Series 1|Ediacaran|Of Amadeus Basin.||||||
12609|Mount Currie Conglomerate|72476|5|Briefly described|p26, 35-36|||Amadeus Basin. Early Paleozoic. Sediments derived from the Musgrave Block basement.|||||Thick (>4 km) packages.|
12609|Mount Currie Conglomerate|73180|6|Mentioned|p48 Fig.1|Early Cambrian|Early Cambrian|Amadeus Basin. Mount spelt as Mt in text.||||Disconformably overlies the Carnegie Formation, underlies the Maurice Formation.||
12639|Mount Doreen Formation|23314|5|Briefly described|331 Fig.2|||||||||
12639|Mount Doreen Formation|24064|4|Described|p226|Adelaidean|Adelaidean|Geological Province: Ngalia Basin. Maximum thicknes: 340m.||||||
12639|Mount Doreen Formation|24111|5|Briefly described|p216|Neoproterozoic|Neoproterozoic|Geological Province: Ngalia Basin. Mount is Mt in text.  See also p215 Fig. 11.||||||30-MAR-05
12639|Mount Doreen Formation|30258|6|Mentioned|p101|||Proterozoic age. See also FIg.2||||||
12639|Mount Doreen Formation|31454|6|Mentioned|Fig.2|||||||||
12639|Mount Doreen Formation|32442|5|Briefly described|p9|||||||||
12639|Mount Doreen Formation|33102|6|Mentioned|Fig.2|||||||||
12639|Mount Doreen Formation|33757|3|Fully described|p9|||See also Table 1. Adelaidean.||||||09-NOV-06
12639|Mount Doreen Formation|33760|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
12639|Mount Doreen Formation|33761|6|Mentioned|p145|||Adelaidean||||||
12639|Mount Doreen Formation|35863|6|Mentioned|p288|||||||||
12639|Mount Doreen Formation|36473|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
12639|Mount Doreen Formation|36898|6|Mentioned|p181|||||||||
12639|Mount Doreen Formation|37462|4|Described|Table 4.IX|||||||||
12639|Mount Doreen Formation|37537|5|Briefly described|Map legend|Adelaidean|Adelaidean|Basal diamictite, pink marker dolomite. Diamictite, dolomite and shale. Geological Province: Ngalia Basin.||||||14-FEB-06
12639|Mount Doreen Formation|37928|3|Fully described|p519|||See also p515.||||||09-NOV-06
12639|Mount Doreen Formation|38157|6|Mentioned|Table VII|||||||||
12639|Mount Doreen Formation|38945|4|Described|p131|||||||||
12639|Mount Doreen Formation|39565|6|Mentioned|p33|||||||||
12639|Mount Doreen Formation|40906|6|Mentioned|Fig.9|||||||||
12639|Mount Doreen Formation|41405|5|Briefly described|p205|||||||||
12639|Mount Doreen Formation|41429|6|Mentioned|p247|||||||||
12639|Mount Doreen Formation|41717|6|Mentioned|Fig.19|||||||||
12639|Mount Doreen Formation|42059|5|Briefly described|Fig.2 P131|||||||||
12639|Mount Doreen Formation|42504|5|Briefly described|p83|||||||||
12639|Mount Doreen Formation|42643|6|Mentioned|p21|||In the Ngalia Basin.||||||09-NOV-06
12639|Mount Doreen Formation|43275|5|Briefly described|Map Legend||Neoproterozoic|||||||
12639|Mount Doreen Formation|43595|5|Briefly described|p548,Fig.5-33,549||Adelaidean|||||||
12639|Mount Doreen Formation|43631|3|Fully described|p24,25||Neoproterozoic|||||||
12639|Mount Doreen Formation|43749|6|Mentioned|Fig.1,p6||Neoproterozoic|||||||
12639|Mount Doreen Formation|44158|4|Described|p29 Table.2|Neoproterozoic|Neoproterozoic|In the Ngalia Basin.||||||09-NOV-06
12639|Mount Doreen Formation|45155|2|Defined|p26|Adelaidean|Adelaidean|||||||
12639|Mount Doreen Formation|46865|4|Described|p52|||Mention p41.||||||09-NOV-06
12639|Mount Doreen Formation|46903|6|Mentioned|p54|||||||||
12639|Mount Doreen Formation|61385|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Tillite, dololutite, shale, sandstone.  Geological Province: Ngalia Basin.||||||
12639|Mount Doreen Formation|62085|6|Mentioned|p24|Ediacaran|Ediacaran|Ngalia Basin. Cap carbonate in this unit corresponds with the GSSP of Nuccaleena Formation.||||||
12639|Mount Doreen Formation|64068|6|Mentioned|p46|||Ngalia Basin.  Correlated with Sun Hill Arkose, Little Burke Tillite, Black Stump Arkose, Wonnadinna Dolostone, Oorabra Arkose, Boko Formation, southern Georgina Basin.||||||
12639|Mount Doreen Formation|65232|5|Briefly described|p70|||Disconformably overlies Rinkabeena Shale. Diamictite, dolostone, shale. Geol. Prov: Ngalia Basin.||||||09-FEB-10
12639|Mount Doreen Formation|65329|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Of Ngalia Basin. Shown as younger than Rinkabeena Shale, older than Yuendumu Sandstone. Tillite, dololutite, shale, sandstone||||||
12639|Mount Doreen Formation|65330|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Of Ngalia Basin. Shown as younger than Rinkabeena Shale, older than Yuendumu Sandstone. Tillite, dololutite, shale, sandstone||||||
12639|Mount Doreen Formation|65342|6|Mentioned|p6.|||Ngalia Basin. Max. thickness at least 149 m.||||Overlies Rinkabeena Shale. Is overlain by Djagamara Formation.|Green to red-brown siltstone.|
12639|Mount Doreen Formation|67872|5|Briefly described|p13, p15, p35|Neoproterozoic|Neoproterozoic|Ngalia Basin. Part of the M2 mega-sequence of Lindsay (2002).|||Wanapi Dolomite Member.|||17-APR-18
12639|Mount Doreen Formation|68244|6|Mentioned|p671|||Ngalia Basin.||||||
12639|Mount Doreen Formation|68270|4|Described|p680,682-683,686-687|Ediacaran|Cryogenian|Ngalia Basin.|||Includes Newhaven Shale Member, Wanapi Dolomite Member and Mount Davenport Diamictite Member.|||
12639|Mount Doreen Formation|68276|6|Mentioned|p73-74|||Ngalia Basin. The barite-rich horizon is overlain by the Red Shale Member.|||Red Shale Member.||Glaciogenic deposits, overlain by seafloor barite associated with ferruginous domal stromatolites.|
12639|Mount Doreen Formation|68277|6|Mentioned|p95|Neoproterozoic|Neoproterozoic|The rank is not given in the text.||||||
12639|Mount Doreen Formation|69437|5|Briefly described|p22:4-5, 7|Ediacaran|Cryogenian|Ngalia Basin, Centralian A Superbasin. Supersequence 3.|||||Diamictite, dolomudstone and shale.|12-JUL-16
12639|Mount Doreen Formation|69438|6|Mentioned|p23:17|||The diamictite member of this unit has been correlated with the Olympic Formation (Amadeus Basin).||||||12-JUL-16
12639|Mount Doreen Formation|69439|4|Described|p24:2-10, 13-14, 16, 18, 20-21|Ediacaran|Ediacaran|Well et al. (1968). Ngalia Basin, Centralian A Superbasin. Supersequence 3. Recessive unit. 100-?350m thick. A complete section is exposed in the Patmungala Syncline, Naburula Hills. Is overlain unconformably by Djagamara Formation and Mount Eclipse Sandstone. Hosts subeconomic amounts of fluorite c.1.6km N of Mount Djagamara. "Oily slicks" were reported from drilling mud during coring of this unit.|||Mount Davenport Diamictite, Wanapi Dolostone, Newhaven Shale, Members.|Unconformably overlies Albinia Formation, Eva Springs Member (Vaughan Springs Quartzite) and (probably) Naburula Formation. Overlies Rinkabeena Shale (probably) disconformably.|Glacial deposits: predominantly diamictite, with subordinate dolostone and shale.|12-JUL-16
12639|Mount Doreen Formation|69443|5|Briefly described|p28:8, 10|||Ngalia Basin. Glacigene and post-glacial deposits related to the Elatina (previously Marinoan) glaciation. Correlates with part of the Mopunga Group (Georgina Basin).||||Equivalent to Keepera Group (Georgina Basin).||12-JUL-16
12639|Mount Doreen Formation|69673|5|Briefly described|p106, p107 fig 85|||Up to 350m thick.|||Includes Mount Davenport Diamictite Member, Wanapi Dolostone Member, Newhaven Shale Member|Overlies Rinkabeena Shale, overlain by Yuendumu Sandstone|Diamictite with subordinate dolostone and shale.|
12639|Mount Doreen Formation|72516|6|Mentioned|p87|Ediacaran|Ediacaran|Ngalia Basin. Age assumed from equivalence with Oorabra Arkose.||||Equivalent to the Oorabra Arkose.||02-JUN-21
12639|Mount Doreen Formation|73086|6|Mentioned|p101, p113, p122, p167|||Ngalia Basin. Upper red shale member may correlate to Pertatataka Formation. Diamictite member correlates with Olympic Formation.||||Correlates to Olympic Formation and Pertatataka Formation.||
12718|Mount Fox adamellite|33224|6|Mentioned|p54|||Permian. Dated c. 265my||||||
12804|Mount Howie Sandstone|13497|5|Briefly described|p115 fig 6.33|Late Cretaceous|Late Cretaceous|||||Unconformably overlies the Winton Formation. Unconformably overlain by the Eyre Formation.||
12804|Mount Howie Sandstone|23054|6|Mentioned|Fig5p22|||||||||
12804|Mount Howie Sandstone|23155|6|Mentioned|Fig 8 on p16||Late Cretaceous|||||||
12804|Mount Howie Sandstone|23818|6|Mentioned|p159|Late Cretaceous|Late Cretaceous|||||||
12804|Mount Howie Sandstone|24175|4|Described|p31, p17 Fig. 3|Coniacian|Turonian|Contains plant fossils.  Disconformably overlies Winton Formation.  Geological Province: Eromanga Basin.||||||
12804|Mount Howie Sandstone|24321|5|Briefly described|Map legend|Turonian|Turonian|Parent: Neales River Group||||||
12804|Mount Howie Sandstone|30803|5|Briefly described|p1|||See also p2-3.||||||31-AUG-20
12804|Mount Howie Sandstone|30804|5|Briefly described|p10|||On Table 1||||||
12804|Mount Howie Sandstone|30807|6|Mentioned|p102|||Suggested map symbol||||||
12804|Mount Howie Sandstone|30919|6|Mentioned|Map legend|Turonian|Turonian|Prob. Turonian||||||
12804|Mount Howie Sandstone|30921|6|Mentioned|Map legend|Turonian|Neocomian|Neocomian - ? Turonian||||||
12804|Mount Howie Sandstone|31706|6|Mentioned|p669|||Cretaceous correlation chart||||||
12804|Mount Howie Sandstone|33820|6|Mentioned|Map legend|Turonian|Turonian|Prob. Turonian||||||
12804|Mount Howie Sandstone|33825|5|Briefly described|p14|||Geol. history||||||
12804|Mount Howie Sandstone|33827|5|Briefly described|p13|||See also p14 & Table 1||||||31-AUG-20
12804|Mount Howie Sandstone|33828|6|Mentioned|p10|||||||||
12804|Mount Howie Sandstone|33938|6|Mentioned|Fig.8|||||||||
12804|Mount Howie Sandstone|34611|5|Briefly described|p159|||See Fig.77||||||
12804|Mount Howie Sandstone|38068|5|Briefly described|p72|||||||||
12804|Mount Howie Sandstone|41085|3|Fully described|p90|||||||||
12804|Mount Howie Sandstone|41535|6|Mentioned|p368|||||||||
12804|Mount Howie Sandstone|42469|6|Mentioned|p35|||||||||
12804|Mount Howie Sandstone|42746|5|Briefly described|p12|||See also Fig.2||||||
12804|Mount Howie Sandstone|42905|5|Briefly described|p21, Fig 5.3|||actually spelt Mt Howie Sandstone||||||
12804|Mount Howie Sandstone|43052|5|Briefly described|Table 2.1|||||||||
12804|Mount Howie Sandstone|43053|5|Briefly described|Map Legend|||Of Mackunda Formation. Coarse channel sand. Spelt Mt Howie Sandstone.||||||25-MAY-05
12804|Mount Howie Sandstone|43258|5|Briefly described|Map Legend||Cretaceous|||||||
12804|Mount Howie Sandstone|43298|5|Briefly described|Map Legend||Cretaceous|spelt Mt Howie Sandstone.||||||
12804|Mount Howie Sandstone|44020|14|Not recorded|p11||Late Cretaceous|||||||
12804|Mount Howie Sandstone|44133|5|Briefly described|p124, 104 Fig. 9.11|Mesozoic|Mesozoic|Geological Province: Eromanga Basin.||||||
12804|Mount Howie Sandstone|65489|5|Briefly described|p96, p155|Late Cretaceous|Late Cretaceous|Eromanga Basin. Appears as Mount Howe Sandstone on p155.||||Unconformably overlies Winton Formation.||
12804|Mount Howie Sandstone|67119|5|Briefly described|Map legend.|Cretaceous|Cretaceous|Is not shown as outcropping in the map area.|||||Medium- to coarse-grained, cross-bedded sandstone.|
12804|Mount Howie Sandstone|69019|5|Briefly described|p85 Fig.21, p102.|Turonian|Turonian|SW and S Eromanga Basin.||||Locally overlies Winton Formation.||
12804|Mount Howie Sandstone|69023|6|Mentioned|p89 Fig.20|Turonian|Turonian|||||||
12804|Mount Howie Sandstone|69946|5|Briefly described|p28, p126-127|||Wopfner (1963), for channel sandstones which he believed incise the Winton Formation. His type section is on the NE slope of Mount Howie, 48km NE of Cordillo Downs. Re-examination of the site showed it to be a facies of the Mackunda Formation; strongly supported by palynological dating. Appears as 'Mt Howie Sandstone': [name to be abandoned?]||||||
12804|Mount Howie Sandstone|70823|5|Briefly described|p43|Late Cretaceous|Late Cretaceous|Eromanga Basin.||||Overlies the Winton Formation.||
12804|Mount Howie Sandstone|71321|6|Mentioned|p15|||Of Eromanga Basin.||||Underlain by Winton Formation.||
12804|Mount Howie Sandstone|71342|5|Briefly described|Ch5 p28, Ch54 p33|Late Cretaceous|Late Cretaceous|Originally defined by Wopfner (1963) as channel sandstone which incise the Winton Formation. Wopfner defined the type section on the northeastern slope of Mount Howie 48 km NE of Cordillo downs. This site, however, was re-examined in 1995 and the sandstone was found to be a facies of the Mackunda Formation, this was strongly supported by palynological dating at the site. Deposited in a fluvio-lacustrine environment. See also Ch5 p128-p129, Ch6 p10.||||||
12804|Mount Howie Sandstone|73106|5|Briefly described|Map legend.|Cretaceous|Cretaceous||||||Sandstone, medium to coarse-grained, cross-bedded.|
12905|Mount Magnificent Loam|38290|5|Briefly described|p58|||||||||
12971|Mount Neill Granite|22631|6|Mentioned|table1, p176|Calymmian|Calymmian|Age: 1569Ma||||||
12971|Mount Neill Granite|23385|6|Mentioned|Table 2|||||||||
12971|Mount Neill Granite|23478|5|Briefly described|p27|Calymmian|Calymmian|Age: 1569+/-14 Ma.||||||
12971|Mount Neill Granite|23775|4|Described|p721-722|Mesoproterozoic|Paleoproterozoic|Spelt 'Mt' in text. Formerly Mount Neill Granite Porphyry. Age: 1569+/-14 Ma, 1576+/-2 Ma, 1575+/-14 Ma. Also see p728-729. Of Older Granite Suite.||||||22-SEP-09
12971|Mount Neill Granite|24197|5|Briefly described|p75 Tb. 8.1|Mesoproterozoic|Mesoproterozoic|Age: 1560Ma.||||||07-FEB-11
12971|Mount Neill Granite|42885|1|Redefined|p28||Mesoproterozoic|redefinition of Coats and Blissett (1971) "Mount Neill Granite Porphyry".||||||25-NOV-22
12971|Mount Neill Granite|43052|5|Briefly described|p151|||supersedes Mount Neill Granite Porphyry||||||
12971|Mount Neill Granite|50605|5|Briefly described|p(ii), 1.4, 10.1, Table 1.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Gawler Craton & Curnamona Province. Of the Babbage supersuite, Moolawatana Suite. Age: 1569 +/- 14Ma (Shrimp).||||||30-AUG-04
12971|Mount Neill Granite|61108|5|Briefly described|map legend|Mesoproterozoic|Mesoproterozoic|Porphyritic granite. Spelt Mt on map legend.||||||21-JUN-05
12971|Mount Neill Granite|61523|6|Mentioned|p12|||Intrusive rocks possibly having a bearing on the mineralisation of the Parabarana copper prospect in the Mount Painter region. Geological Province: Mount Painter Province.||||||30-APR-10
12971|Mount Neill Granite|62962|5|Briefly described|p2284 Fig. 2|Mesoproterozoic|Mesoproterozoic|Age: 1569+/-14Ma (Teale 1987, unpub. data. U/Pb SHRIMP).||||||12-NOV-14
12971|Mount Neill Granite|63866|6|Mentioned|p43|||||||||
12971|Mount Neill Granite|64722|5|Briefly described|Fig. 2 p3-6, p15|Calymmian|Calymmian|With the Petermorra Volcanics, part of a succession of felsic volcanic and intrusive rocks that range in age from 1780-1550 Ma and overlie the Radium Creek Metamorphics. Has a within-plate geochemical signature.||||||
12971|Mount Neill Granite|65925|5|Briefly described|p128, Appendix 2.|||A probable metavolcanic unit; part of the Mount Painter Inlier basement in the Arkaroola area.|c.1575 Ma.|||Is unconformably overlain by Paralana Quartzite.|Red-brown, quartz-muscovite-feldspar unit with rounded blue quartz phenocrysts.|
12971|Mount Neill Granite|66302|6|Mentioned|p49, p52, p78|Calymmian|Calymmian|Moolawatana Domain, Curnamona Province. Ages are derived from Fanning (1998) and Fraser and Neumann (2010), respectively.|1569 +/- 14 Ma  to 1585 +/-3 Ma|||||
12971|Mount Neill Granite|66518|6|Mentioned|p19 Fig.4.|Mesoproterozoic|Mesoproterozoic|Curnamona Province.|c.1580 Ma.|||||
12971|Mount Neill Granite|67430|6|Mentioned|p56|||Mount Gee - Mount Painter area, Mount Painter Inlier.||||||
12971|Mount Neill Granite|67536|5|Briefly described|Map Legend|Calymmian|Calymmian|Curnamona Province. Written as Mt Neill Granite in text.|1569 +/- 14 Ma.||||Porphyritic granite.|
12971|Mount Neill Granite|67540|3|Fully described|p25, pp27-28, p36 Tb.3, p40 Fig.2|Calymmian|Calymmian|Type locality ~350 m NNW of Mount Neil [sic]; a subsidiary type locality is along a creek section ~1700 m SSW of Mount Adams. Curnamona Province, Moolatawatana Domain. Is considered to be the intrusive equivalent of Pepegoona Porphyry.|1585-1569 Ma|Of the Coulthard Suite.||Faulted against and/or intrudes Radium Creek Metamorphics and Box Bore Granite. Is coeval with Pepegoona Porphyry.|Undeformed, brick red to grey, medium- to coarse-grained microcline, quartz and muscovite granites with massive to fine-grained equivalents. A-type.|08-FEB-16
12971|Mount Neill Granite|67581|6|Mentioned|p45|||Curnamona Province.||||||
12971|Mount Neill Granite|67653|6|Mentioned|p4|||Geological province: Curnamona Province.||||||
12971|Mount Neill Granite|68068|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Curnamona Province. Formerly the Mount Neill Granite Porphyry.|1569 +/- 14 Ma (U-Pb zircon).|||Intrudes Radium Creek Metamorphics.|Massive, grey, porphyritic, coarse-grained granite with minor adamellite; broad chilled margin of porphyritic microgranite; includes minor ?extrusive equivalents, very weakly deformed to undeformed.|11-NOV-13
12971|Mount Neill Granite|68126|6|Mentioned|p6|||Mount Painter Inlier, Curnamona Province.||||||
12971|Mount Neill Granite|69019|5|Briefly described|p30 Fig.10.|Calymmian|Calymmian|Mt. Painter Inlier. See also references to Mount Neill Granite Porphyry (p20, p27-29 Figs.7-9).|c.1570 Ma.|||||
12971|Mount Neill Granite|69023|5|Briefly described|p15, p21-22, p24-27, p43, p52-54, p145|Mesoproterozoic|Mesoproterozoic|See also p159-160, p189, p202. Originally Mount Neill Granite Porphyry (Coats and Blissett, 1971); subsequently Mount Neill Granite (Teale, 1993), excluding Petermorra Volcanics. An intricately complex intrusive-subvolcanic rock body. Geochemistry detailed.|1569 +/- 14 Ma U-Pb zircon (Fanning, 1995).|||Intrudes Radium Creek Metamorphics.|Medium- to coarse-grained, porphyritic to megacrystic (K-feldspar, quartz, biotite), granite; occasional weak foliation. A-type.|
12971|Mount Neill Granite|69562|5|Briefly described|p669, p670 Tb.5, p673 Fig.5, p683-684|||Mount Painter Inlier. Contains 3 to 380 ppm U: excellent source of leachable U.|1585 +/- 3 Ma (Fraser and Neumann, 2010).|Unit in Coulthard Suite.|||Coarse-grained granite.|
12971|Mount Neill Granite|69650|1|Redefined|p4 Tb.1, p8-9, p11, p13, p57-65, p68|Calymmian|Calymmian|See also p70-71, p73-75. Originally Mount Neill Granite Porphyry of Coats and Blissett (1971); revised to present name and defined by Teale (1993). Named after Mount Neil [sic], near Arkaroola. Type localities:Type Locality: at approximately 350 m NNW of Mount Neil at GDA94, 367000 mE, 6677320 mN (Fig. 31); and a subsidiary type locality exposed along a creek section approximately 1700 m SSW of Mt Adams (Coats and Blissett, 1971). Crops out extensively within Mount Painter Inlier as laccoliths, sills and lenses. Considered as the intrusive equivalent of Pepegoona Porphyry and coeval with Box Bore Granite. Nooldoonooldoona Trondhjemite may be a metasomatised variant of this unit (Elburg et al.,2001). Geochronology, geochemistry detailed.|1590-c.1569 Ma.|Unit in Coulthard Suite.||Faulted against and/or intrudes Radium Creek Metamorphics and Box Bore Granite.|Undeformed, brick-red to grey, medium- to coarse-grained microcline-quartz-muscovite granites with massive to fine-grained equivalents. A-type.|25-NOV-22
12971|Mount Neill Granite|69654|6|Mentioned|p3|||Curnamona Province.||||||
12971|Mount Neill Granite|70384|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Four intermediate age determinations are provided.|1590 +/- 5 (ICPMS) to 1569 +/- 14 Ma (SHRIMP).|Coulthard Suite.|||Massive, grey, microcline-phyric, coarse-grained granite with minor adamellite. Broad chilled margins of porphyritic microgranite; unit includes minor ?extrusive equivalents, very weakly deformed to undeformed. A-type.|
12971|Mount Neill Granite|70658|5|Briefly described|p33-35, 37|Mesoproterozoic|Mesoproterozoic|Curnamona Province. Geochemistry briefly described. Forms laccoliths, sills and lenses. Extensive outcrops in the Mount Painter Inlier.|1585 - c.1569 Ma.|Coulthard Suite.|||Undeformed, brick-red to grey, medium- to coarse-grained microcline, quartz and muscovite granites with massive to fine-grained equivalents. A-type.|
12971|Mount Neill Granite|72456|6|Mentioned|Solid Geology Interpretation|||||||||
12971|Mount Neill Granite|72949|6|Mentioned|p36|Calymmian|Calymmian|Curnamona Province. Mount Painter.|1590-1569 Ma|||||
12971|Mount Neill Granite|73061|4|Described|p1067-1069, p1071-1073, p1076|Calymmian|Calymmian|Mount Painter Province, Mount Painter Inlier. Written as Mt Neill Granite in text. High heat producing granite. Cross-cuts foliation developed in the Radium Creek Metamorphics. Overlap in age with Pepegoona Volcanics interpreted as indicating they formed in the same magmatic event. 1569 +/- 14 Ma age of Fanning (1995) may reflect later metamorphism and deformation. Mean eHf value of +1.4 +/- 0.6. Crosscut by andesitic dyke (1571 +/- 5 Ma crystallisation age). The Box Bore Granite may possibly be associated as a strongly deformed zone. Location in text includes p1070 Tb.1, Fig.2, p1074 Fig.4.|1590 +/- 5 Ma U-Pb LA-ICPMS, 1585 +/- 3 Ma|||Intrudes the Radium Creek Metamorphics.|Includes medium-grained, pink granite with rounded feldspar and rounded blue quartz phenocrysts, deformed in places.|
12971|Mount Neill Granite|73251|6|Mentioned|p35-36|Calymmian|Calymmian|Curnamona Province, Mount Painter and Mount Babbage inliers. Includes uraniferous crystalline rock.|c. 1580 Ma|||||
12992|Mount Painter Complex|9862|5|Briefly described|Map Legend|Precambrian|Precambrian|Sericitic quartzite with heavy mineral lamination. Granitized sediments and migmatitic granite. Rapakivi granite and other granitic rocks.||||||
12992|Mount Painter Complex|22725|6|Mentioned|p243|||Mount spelled Mt in text.||||||
12992|Mount Painter Complex|23394|5|Briefly described|Map legend|Proterozoic|Proterozoic|||||||
12992|Mount Painter Complex|23411|6|Mentioned|Map Legend|||||||||
12992|Mount Painter Complex|23412|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Mount is Mt. in text||||||
12992|Mount Painter Complex|23818|6|Mentioned|p64 Fig.22|||Overlying unit: Yudnamutana Sub-Group (unconformable).||||||
12992|Mount Painter Complex|24138|4|Described|p10-14|Precambrian|Precambrian|Age: c. 1600 Ma. Mainly granites and metamorphics. Written Mt in text. Forms basement for Adelaide Geosyncline.||||||
12992|Mount Painter Complex|29840|6|Mentioned|p504|||||||||
12992|Mount Painter Complex|30176|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Prob.Lower Proterozoic||||||07-NOV-08
12992|Mount Painter Complex|30178|6|Mentioned|p20|||||||||
12992|Mount Painter Complex|30261|6|Mentioned|Table 1|||||||||
12992|Mount Painter Complex|30920|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
12992|Mount Painter Complex|31109|6|Mentioned|p8|||Map.||||||
12992|Mount Painter Complex|31541|6|Mentioned|p544|||||||||
12992|Mount Painter Complex|31923|6|Mentioned|p6|||||||||
12992|Mount Painter Complex|33472|6|Mentioned|p470|||||||||
12992|Mount Painter Complex|33969|5|Briefly described|p506|||||||||
12992|Mount Painter Complex|34287|6|Mentioned|p35|||||||||
12992|Mount Painter Complex|34535|6|Mentioned|Fig.22|||||||||
12992|Mount Painter Complex|34720|6|Mentioned|p329|||||||||
12992|Mount Painter Complex|34726|6|Mentioned|p101|||||||||
12992|Mount Painter Complex|34812|6|Mentioned|Table 8|||||||||
12992|Mount Painter Complex|35255|6|Mentioned|p41|||||||||
12992|Mount Painter Complex|35327|6|Mentioned|Fig.1|||||||||
12992|Mount Painter Complex|36194|6|Mentioned|p575|||||||||
12992|Mount Painter Complex|37325|6|Mentioned|p7|||||||||
12992|Mount Painter Complex|37461|6|Mentioned|Table 5.I|||||||||
12992|Mount Painter Complex|37799|5|Briefly described|p115|||||||||
12992|Mount Painter Complex|37854|6|Mentioned|Table 1|||||||||
12992|Mount Painter Complex|37932|6|Mentioned|p539|||||||||
12992|Mount Painter Complex|39352|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
12992|Mount Painter Complex|39872|6|Mentioned|Table 2|||||||||
12992|Mount Painter Complex|40294|6|Mentioned|Table 1|||||||||
12992|Mount Painter Complex|40490|6|Mentioned|Table I|||||||||
12992|Mount Painter Complex|40950|6|Mentioned|p251|||||||||
12992|Mount Painter Complex|41038|5|Briefly described|p314|||||||||
12992|Mount Painter Complex|41125|6|Mentioned|p10|||See also P49 and Fig.20||||||
12992|Mount Painter Complex|41228|5|Briefly described|p858|||||||||
12992|Mount Painter Complex|41403|6|Mentioned|p43|||See also Fig.11||||||
12992|Mount Painter Complex|41526|6|Mentioned|p27|||||||||
12992|Mount Painter Complex|41647|6|Mentioned|Fig.2|||||||||
12992|Mount Painter Complex|41770|6|Mentioned|p242|||||||||
12992|Mount Painter Complex|43591|6|Mentioned|p184|||||||||
12992|Mount Painter Complex|61556|5|Briefly described|p9-10 Figure|Paleoproterozoic|Paleoproterozoic|In the Flinders ranges, Adelaide Syncline.||||||07-NOV-08
12992|Mount Painter Complex|64329|5|Briefly described|p18|||Intruded by Palaeozoic granitoids. Large bodies of breccia, the Radium Ridge breccias, occur within the complex.||||||
12992|Mount Painter Complex|65925|5|Briefly described|p124 Fig.3.||||||||Granite, porphyry, quartzite, metasediments.|
12992|Mount Painter Complex|71531|14|Not recorded|p8, 9 |||||||||
13080|Mount Salt Formation|12796|4|Described|p461, p456 Fig. 2|Santonian|Coniacian|Of Sherbrook Group. Name revived to reduce or eliminate diachronism. Interfingers with and overlies Morum Formation. Geological Province: Otway Basin/Gambier Embayment.||||||
13080|Mount Salt Formation|22470|5|Briefly described|p13 Fig. 17|Santonian|Coniacian|Of Sherbrook Group.||||||
13080|Mount Salt Formation|24562|6|Mentioned|p42 Fig. 15|||Of the Otway Group.  Geological Province: Otway Basin.||||||
13080|Mount Salt Formation|33165|6|Mentioned|Chart|||Correlation chart only||||||
13080|Mount Salt Formation|48911|3|Fully described|p19|||Uppermost L.Cret. to Upper Cret.||||||
13080|Mount Salt Formation|61625|6|Mentioned|p476|||||||||07-FEB-11
13080|Mount Salt Formation|69297|6|Mentioned|p79|Santonian|Coniacian|Otway Basin.||||Overlies the Mourum Member. Overlain by the Paaratte Formation.|Mudstone and siltstone.|
13080|Mount Salt Formation|70077|5|Briefly described|Nelson: Fig.2. Regional: Fig.4|Late Cretaceous|Late Cretaceous|Otway Basin: Gambier Embayment and Voluta Trough.||Sherbrook Group.||Overlies Flaxman Formation. Is overlain by Paaratte Formation. Is equivalent to Belfast Mudstone.||
13080|Mount Salt Formation|70078|5|Briefly described|Northern: Fig.2. Regional: Fig.4|Santonian|Coniacian|Gambier Embayment and Voluta Trough.||Sherbrook Group.||Overlies Belfast Mudstone or Flaxman Formation. Is overlain by Paaratte Formation.||
13080|Mount Salt Formation|73357|6|Mentioned|p20-21|Santonian|Coniacian|Otway Basin. The C. vultuosus Subzone (Phyllocladidites mawsonii Spore-Pollen Zone) resides within the Mount Salt Formation or its equivalents in South Australia. Mount Salt Formation equivalents are correlated with I. cretaceum Dinocyst Zone, C. striatoconum Dinocyst Zone, O.porifera Dinocyst Zone and T. apoxyexinus Spore-Pollen Zone in the western onshore Otway Basin. See also discussion of equivalents p47.||Of Sherbrook Group.||The Mount Salt Formation equivalent overlies Flaxman Formation, underlies Paaratte Formation.||
13088|Mount Sarah Sandstone|29660|2|Defined|p4|Miocene|late Oligocene|Late Oligocene to Mid Pliocene||||||
13088|Mount Sarah Sandstone|35080|6|Mentioned|p9|||||||||
13088|Mount Sarah Sandstone|36966|6|Mentioned|p81|||||||||
13088|Mount Sarah Sandstone|38022|6|Mentioned|p66|||||||||
13088|Mount Sarah Sandstone|38605|6|Mentioned|p35|||See also Table 5.||||||
13088|Mount Sarah Sandstone|39322|6|Mentioned|Fig.3|||||||||
13088|Mount Sarah Sandstone|40925|6|Mentioned|Map legend|Cenozoic|Cenozoic|||||||19-NOV-08
13088|Mount Sarah Sandstone|40926|3|Fully described|p22|||||||||
13088|Mount Sarah Sandstone|43048|6|Mentioned|p22|||||||||
13088|Mount Sarah Sandstone|43053|5|Briefly described|Map Legend|Pleistocene|Tertiary|Spelt Mt Sarah Sandstone. Undifferentiated Early Tertiary to Plio-Pleistocene alluvial, colluvial and residual clastics, commonly silicified or ferruginised.||||||25-MAY-05
13088|Mount Sarah Sandstone|43071|6|Mentioned|p17|||||||||
13088|Mount Sarah Sandstone|43258|5|Briefly described|Map Legend|Pliocene|Paleocene|spelt Mt.Sarah Sandstone.||||||
13088|Mount Sarah Sandstone|43298|6|Mentioned|Map Legend|Pleistocene|Tertiary|spelt Mt Sarah Sandstone.||||||
13088|Mount Sarah Sandstone|44133|5|Briefly described|p193, 190 Fig. 10.30|Middle Eocene|Middle Eocene|Geological Province: Lake Eyre Basin.||||||
13088|Mount Sarah Sandstone|60953|5|Briefly described|Map Legend|Miocene|Eocene|Alluvial, colluvial and residual clastics, commonly silicified or ferruginised.||||||27-APR-05
13088|Mount Sarah Sandstone|61155|5|Briefly described|p17|Middle Miocene|Early Miocene|Geological region: Oodnadatta area. Mount is Mt in text of chart.||||||
13088|Mount Sarah Sandstone|66131|6|Mentioned|p240, p242 Fig.2|Eocene|Eocene|Colluvial facies and elevated sinuous palaeochannel sand and gravel. Tirari Sub-basin. Age from Fig.2 - stratigraphic correlation chart. Middle Eocene.||||Equivalent to Eyre Formation.||
13088|Mount Sarah Sandstone|66623|6|Mentioned|p273.|||Tirari sub-basin, South Australia. Part equivalent to Eyre Formation.||||||
13088|Mount Sarah Sandstone|69019|6|Mentioned|p105 Fig.25.|Eocene|Eocene|Tirari Sub-basin.||||||
13088|Mount Sarah Sandstone|69023|6|Mentioned|p108|Eocene|Eocene|Callabonna Sub-basin, Lake Eyre Basin.||||||
13088|Mount Sarah Sandstone|70336|5|Briefly described|Map legend|Oligocene|Eocene||||||Cross-bedded sandstone, siltstone and cross-bedded basal conglomerate. Channel facies.|
13097|Mount Shannan Iron Formation|23719|4|Described|p14|Paleoproterozoic|Paleoproterozoic|Also known as Upper Middleback Jaspilite. See also page 14 Table 1. Of Middleback Subgroup. O'lying unit Yadnarie Schist. U'lying unit Cook Gap Schist. Geol. Province: Gawler Craton. Max. thickness: >200 m.||||||07-NOV-08
13097|Mount Shannan Iron Formation|37811|6|Mentioned|p233|||Local name.||||||
13097|Mount Shannan Iron Formation|39345|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
13097|Mount Shannan Iron Formation|39349|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
13097|Mount Shannan Iron Formation|39353|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
13097|Mount Shannan Iron Formation|40448|6|Mentioned|Table 1|||||||||
13097|Mount Shannan Iron Formation|41667|5|Briefly described|p55|||||||||
13097|Mount Shannan Iron Formation|43052|5|Briefly described|p57|||see also Fig.4.4. Synonym for Upper Middleback Jaspilite||||||
13097|Mount Shannan Iron Formation|62893|6|Mentioned|Map Legend, p11|Early Proterozoic|Early Proterozoic|Local name for the Upper Middleback Jaspilite.||||||
13133|Mount Terrible Formation|22643|5|Briefly described|fig3p187|Early Cambrian|Early Cambrian|Spelt"Mt" in the text||||||
13133|Mount Terrible Formation|22766|4|Described|Fig.2 p561, p562|Tommotian|Tommotian|Spelt Mt Terrible Formation||||||
13133|Mount Terrible Formation|22857|5|Briefly described|p88 Fig. 14.7A|Early Cambrian|Early Cambrian|Of the Normanville Group. Mount is Mt. in text of figure. Geological Province: Kanmantoo Trough.||||||
13133|Mount Terrible Formation|22858|6|Mentioned|Fig14.7ap88-9|Tommotian|Tommotian|||||||
13133|Mount Terrible Formation|23818|5|Briefly described|p87 Fig.33|Cambrian|Cambrian|Mount is spelt Mt. in text.||||||
13133|Mount Terrible Formation|23854|5|Briefly described|p864|Early Cambrian|Early Cambrian|Mount is Mt. in text. Of Normanville Group.||||||
13133|Mount Terrible Formation|23981|5|Briefly described|p8-9 Fig. 4, p10 Fig. 5|Tommotian|Precambrian|Basal clastics of Normanville Gp. Overlies Marino Gp; underlies Wangkonda Fm. Thickness:15m. Geol.Prov: Stansbury Basin. Coarse-gr.arkose passing rapidly up into shallow marine bioturb.siltstone and fossiliferous, silty calcareous sst. Mount is Mt in text.||||||12-DEC-21
13133|Mount Terrible Formation|24465|5|Briefly described|p358|Early Cambrian|Early Cambrian|Of Normanville Group. Geological Province: Stansbury Basin.  Mount is Mt in text.||||||27-MAY-08
13133|Mount Terrible Formation|30049|4|Described|p43|||See also p44, Fig.1, Fig.2 Cambrian age.||||||01-JUL-08
13133|Mount Terrible Formation|30052|6|Mentioned|Fig.3|||Cambrian age.||||||
13133|Mount Terrible Formation|30220|6|Mentioned|Fig.13|||||||||
13133|Mount Terrible Formation|30374|6|Mentioned|Fig.5|||Correlation. Lower Cambrian age||||||
13133|Mount Terrible Formation|30377|6|Mentioned|p200|||Lower Cambrian age||||||
13133|Mount Terrible Formation|30378|6|Mentioned|p432|||See also Table 1. Lower Cambrian age||||||
13133|Mount Terrible Formation|30379|5|Briefly described|p90|||Cambrian age||||||
13133|Mount Terrible Formation|30381|6|Mentioned|p222|||||||||
13133|Mount Terrible Formation|30801|6|Mentioned|p5|||Lower Cambrian. Table P5-6.||||||
13133|Mount Terrible Formation|30805|6|Mentioned|p1|||||||||
13133|Mount Terrible Formation|30807|6|Mentioned|p102|||Suggested map symbol||||||
13133|Mount Terrible Formation|32551|6|Mentioned|p100|||Camb. lithology||||||
13133|Mount Terrible Formation|32724|6|Mentioned|Fig.1|||Cambrian. Correlation||||||
13133|Mount Terrible Formation|33332|6|Mentioned|p10|||L.Camb.||||||
13133|Mount Terrible Formation|33470|6|Mentioned|Table 1|||||||||
13133|Mount Terrible Formation|33471|6|Mentioned|Fig.1|||||||||
13133|Mount Terrible Formation|33953|6|Mentioned|Fig.4|||Cambrian||||||
13133|Mount Terrible Formation|34014|5|Briefly described|p22|||Cambrian||||||
13133|Mount Terrible Formation|34021|4|Described|p95|||L.Cambrian||||||
13133|Mount Terrible Formation|34536|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
13133|Mount Terrible Formation|34612|6|Mentioned|Fig.33|||Cambrian. Correlation chart.||||||
13133|Mount Terrible Formation|34911|6|Mentioned|p86|||||||||
13133|Mount Terrible Formation|34959|6|Mentioned|p284|||||||||
13133|Mount Terrible Formation|35255|6|Mentioned|Fig.4|||See also Fig.8.||||||
13133|Mount Terrible Formation|35678|6|Mentioned|p64|||Summary geological logs.||||||
13133|Mount Terrible Formation|38873|6|Mentioned|Table 2|||||||||
13133|Mount Terrible Formation|39489|6|Mentioned|p8|||||||||
13133|Mount Terrible Formation|39806|6|Mentioned|p207|||||||||
13133|Mount Terrible Formation|40442|6|Mentioned|p10|||||||||
13133|Mount Terrible Formation|40455|5|Briefly described|p67|||||||||
13133|Mount Terrible Formation|40810|5|Briefly described|p13|||||||||
13133|Mount Terrible Formation|40852|6|Mentioned|p32|||||||||
13133|Mount Terrible Formation|40856|5|Briefly described|p312|||||||||
13133|Mount Terrible Formation|41103|6|Mentioned|Fig.1|||||||||
13133|Mount Terrible Formation|42192|6|Mentioned|p4|||||||||
13133|Mount Terrible Formation|42222|6|Mentioned|p20|||||||||
13133|Mount Terrible Formation|42225|6|Mentioned|Fig.4 P224|||||||||
13133|Mount Terrible Formation|42232|6|Mentioned|p269|||||||||
13133|Mount Terrible Formation|42235|5|Briefly described|p140|||||||||
13133|Mount Terrible Formation|42242|6|Mentioned|p200|||||||||
13133|Mount Terrible Formation|42266|5|Briefly described|p290|||||||||
13133|Mount Terrible Formation|42270|6|Mentioned|p353|||||||||
13133|Mount Terrible Formation|42488|5|Briefly described|Fig.2 P187|||||||||
13133|Mount Terrible Formation|43052|5|Briefly described|Table 2.1|||||||||
13133|Mount Terrible Formation|43703|6|Mentioned|Fig.1,p75|||||||||
13133|Mount Terrible Formation|43781|6|Mentioned|p8|||||||||
13133|Mount Terrible Formation|44133|5|Briefly described|p4 Fig. 7.2, 6, 7|Early Cambrian|Early Cambrian|Geological Province: Stansbury Basin. Of the Normanville Group. Discordantly overlies: lower Wilpena Group.||||||
13133|Mount Terrible Formation|44690|4|Described|map legend||Cambrian|Geol. Atlas Series. (I/54-5). Marginal shelf deposit.||||||03-MAY-13
13133|Mount Terrible Formation|45102|6|Mentioned|p48|||||||||
13133|Mount Terrible Formation|60712|5|Briefly described|p28 Fig. 1|Early Cambrian|Early Cambrian|Of the Normanville Group.||||||31-MAY-05
13133|Mount Terrible Formation|60889|5|Briefly described|p245 Fig.2|Early Cambrian|Early Cambrian|Shown as Mt Terrible Formation. Contains small shelly fossil assemblages (Bemella Watsonella). Arrowie Basin.||||||
13133|Mount Terrible Formation|61307|5|Briefly described|p6 Fig. 3|Cambrian|Cambrian|Of the Normanville Group. Geological Province: Adelaide Fold Belt. Mount is Mt in text of figure.||||||15-JAN-08
13133|Mount Terrible Formation|63848|6|Mentioned|p534 Fig.4.|||||Unit in Normanville Group.||Is overlain by Wangkonda Formation.||
13133|Mount Terrible Formation|64282|5|Briefly described|Map legend|Early Cambrian|Early Cambrian|Metasiltstone with actinolite-rich bands and calc-silicate rock; basal 2m thick arkosic band. On Dudley Peninsula. Mount is Mt in text of legend.||||||01-JUL-08
13133|Mount Terrible Formation|65375|5|Briefly described|p33.|Early Cambrian|Early Cambrian|||Unit in Normanville Group.||Is overlain by Wangkonda Formation.||
13133|Mount Terrible Formation|65686|6|Mentioned|p415|Early Cambrian|Early Cambrian|||||||
13133|Mount Terrible Formation|65892|4|Described|p7 Fig.3, p9 Fig.4, p13-16. |Early Cambrian|Early Cambrian|Fleurieu Peninsula. Type area near Sellick Hill. Comprises three members totalling 85m thickness.||Oldest unit in Normanville Group.||Overlies, and fills small hollows cut into, Marino Group. Is overlain conformably by Wangkonda Formation.|Coarse-grained cross-bedded feldspathic sandstone and arkose; bioturbated siltstone with phosphatic concretions; feldspathic bioturbated sandstone with cavernous weathering of small calcareous lenses.|
13133|Mount Terrible Formation|66761|6|Mentioned|p254|Terreneuvian|Terreneuvian|Underlies the Wangkonda Formation. Fleurieu Peninsula.||||||14-MAR-12
13133|Mount Terrible Formation|68735|5|Briefly described|p233 Fig.2, p235 Fig.3|Early Cambrian|Early Cambrian|Stansbury Basin. Mount spelt as Mt in text.||Of the Normanville Group.||||
13133|Mount Terrible Formation|68993|6|Mentioned|p544 Fig.1|Early Cambrian|Early Cambrian|Fleurieu Peninsula. Spelt as Mt Terrible Formation in the text.||Of the Normanville Group.||||
13133|Mount Terrible Formation|70833|5|Briefly described|p200|Cambrian|Cambrian|Of Eastern Stansbury Basin.||||Overlain unconformably by Wangkonda Formation.||
13133|Mount Terrible Formation|71237|14|Not recorded|p9|||||||||
13133|Mount Terrible Formation|71238|14|Not recorded|p3, p9||Cambrian|||||||
13133|Mount Terrible Formation|71241|14|Not recorded|p15, p9|||Of Daily (1963).||||Overlies Pound Quartzite, overlain by Kulpara Limestone. Equivalent to Parachilna Formation.|Thin arkosic unit.|
13133|Mount Terrible Formation|72450|5|Briefly described|Brochure map||||c. 520 Ma|Normanville Group|||Arkosic grit, overlain by siltstone and sandstone.|
13133|Mount Terrible Formation|73059|6|Mentioned|p1061|||||Normanville Group.||||
13133|Mount Terrible Formation|73093|5|Briefly described|map legend|Cambrian|Cambrian||||||Arkose, cross-bedded, coarse-grained to conglomeratic, pyritic and glauconitic sandstone, minor shale siltstone and dolomite.|09-DEC-21
13133|Mount Terrible Formation|73107|5|Briefly described|Map legend.|Early Cambrian|Early Cambrian|Dudley Peninsula.|||||Metasiltstone with actinolite rich bands and calc-silicate rock. Basal 2m thick arkosic band.|
13133|Mount Terrible Formation|73188|6|Mentioned|p316|Early Cambrian|Early Cambrian|Mount Lofty Ranges.||Normanville Group|||Arkose, siltstone, sandstone.|
13133|Mount Terrible Formation|73247|6|Mentioned|p205|Cambrian (Stage 2)|Cambrian (Stage 2)|Fleurieu Peninsula.||||Overlain by Wangkonda Formation. Equivalent to Winulta Formation.||
13133|Mount Terrible Formation|73264|6|Mentioned|p1387 Fig.10, p1394|||Normanville Shelf. Shown as Mt Terrible Formation in text.||Normanville Group||||
13151|Mount Toondina Formation|13516|6|Mentioned|p147, fig 5|Early Permian|Early Permian|From Arkaringa Basin||||||
13151|Mount Toondina Formation|22922|6|Mentioned|33 fig 2|||Mount spelt as 'Mt' in text||||||
13151|Mount Toondina Formation|23054|4|Described|p18-20,36,Fig9p37||Sakmarian|||||||
13151|Mount Toondina Formation|23282|6|Mentioned|p84 Fig 6.2|||of Arckaringa Basin.||||||
13151|Mount Toondina Formation|23288|6|Mentioned|Fig.5||Early Permian|of Marla area.||||||
13151|Mount Toondina Formation|23829|5|Briefly described|p371|Permian|Permian|Geological Province: Arckaringa Basin.||||||
13151|Mount Toondina Formation|24112|5|Briefly described|p270-271, p257, p263, 268|Permian|Permian|Mount is Mt. in text. Age: 270-260Ma [no reason or timescale given]. Geological Province: Arckaringa Basin||||||19-SEP-18
13151|Mount Toondina Formation|30924|6|Mentioned|Map legend|Artinskian|Artinskian|||||||
13151|Mount Toondina Formation|32033|6|Mentioned|p2|||||||||
13151|Mount Toondina Formation|33523|4|Described|p24|||||||||
13151|Mount Toondina Formation|33525|2|Defined|p2|Permian|Permian|||||||
13151|Mount Toondina Formation|33942|6|Mentioned|p21|||||||||
13151|Mount Toondina Formation|33971|6|Mentioned|Fig.18|||||||||
13151|Mount Toondina Formation|33976|6|Mentioned|p9|||Similar to Purni Formation.||||||
13151|Mount Toondina Formation|35149|5|Briefly described|Table 1|||||||||
13151|Mount Toondina Formation|35315|6|Mentioned|Fig.2|||||||||
13151|Mount Toondina Formation|35845|6|Mentioned|Fig.25|||||||||
13151|Mount Toondina Formation|36733|6|Mentioned|p14|||||||||
13151|Mount Toondina Formation|37855|6|Mentioned|Fig.2|||||||||
13151|Mount Toondina Formation|38022|6|Mentioned|Fig.4|||||||||
13151|Mount Toondina Formation|38604|6|Mentioned|Map legend|Permian|Carboniferous|Carboniferous - Permian||||||
13151|Mount Toondina Formation|38605|4|Described|p19|||See also Table 3.||||||
13151|Mount Toondina Formation|38958|5|Briefly described|p491|||||||||
13151|Mount Toondina Formation|39265|6|Mentioned|Fig. 3|||||||||
13151|Mount Toondina Formation|39352|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
13151|Mount Toondina Formation|40637|6|Mentioned|Fig.2|||||||||
13151|Mount Toondina Formation|41183|6|Mentioned|Fig.3 p308|||||||||
13151|Mount Toondina Formation|41491|4|Described|p171|||||||||
13151|Mount Toondina Formation|41689|6|Mentioned|Table 1|||||||||
13151|Mount Toondina Formation|41950|6|Mentioned|Fig.3 P4|||||||||
13151|Mount Toondina Formation|42102|6|Mentioned|p86|||||||||
13151|Mount Toondina Formation|42469|6|Mentioned|p27, p30, p55|||||||||
13151|Mount Toondina Formation|42546|5|Briefly described|Map legend|Permian|Carboniferous|||||||
13151|Mount Toondina Formation|42578|6|Mentioned|Table 1 P124-125|||Actually spelt Mt. Toondina Fm.||||||
13151|Mount Toondina Formation|42723|5|Briefly described|map legend|Permian||||||||
13151|Mount Toondina Formation|42736|5|Briefly described|map legend|Permian|Carboniferous|||||||
13151|Mount Toondina Formation|42816|6|Mentioned|p17|||||||||
13151|Mount Toondina Formation|43048|4|Described|Table 2.|||||||||
13151|Mount Toondina Formation|43052|5|Briefly described|Table 2.1|||||||||
13151|Mount Toondina Formation|43053|5|Briefly described|Map Legend|Permian|Carboniferous|Geological Province: Arckaringa Basin.||||||25-MAY-05
13151|Mount Toondina Formation|43258|5|Briefly described|Map Legend|Permian|Carboniferous|spelt Mt Toondina Formation||||||
13151|Mount Toondina Formation|43298|6|Mentioned|Map Legend|Permian|Carboniferous|spelt Mt Toodina Formation.||||||
13151|Mount Toondina Formation|43657|6|Mentioned|Fig.3,p4|Permian|Carboniferous|||||||
13151|Mount Toondina Formation|43690|6|Mentioned|Fig.2,p157|||||||||
13151|Mount Toondina Formation|43743|6|Mentioned|Fig.2,p33||Early Permian|||||||
13151|Mount Toondina Formation|43840|4|Described|p11, Fig3 p12||Early Permian|Contains a total of 25m of coal||||||12-JUL-16
13151|Mount Toondina Formation|44109|5|Briefly described|p22 Fig. 30|Permian||Geological Province: central Officer Basin. Mount is Mt in text of figure.||||||
13151|Mount Toondina Formation|44133|5|Briefly described|p65 Fig. 8.3, 73, 75|Artinskian|Sakmarian|Geological Province: Arckaringa Basin. Overlies: Stuart Range Formation.||||||
13151|Mount Toondina Formation|44289|5|Briefly described|Map Legend||Sakmarian|||||||
13151|Mount Toondina Formation|44935|5|Briefly described|Map Legend|Permian|Carboniferous|Arckaringa Basin and Mulgathing Trough||||||
13151|Mount Toondina Formation|60953|5|Briefly described|Map Legend|Permian|Carboniferous|Geological Province: Arkaringa Basin.||||||19-SEP-18
13151|Mount Toondina Formation|61108|5|Briefly described|map legend|Permian|Carboniferous|Spelt Mt on map legend. Glaciomarine, fluvioglacial and fluviolacustrine till, clay, silt, sand and gravel, indurated and coal-bearing in Ackaringa Basin. Geological Province: Arckaringa Basin.||||||02-JUN-05
13151|Mount Toondina Formation|65489|5|Briefly described|p137, p143, p151|Permian|Permian|Arckaringa Basin. 600m thick. Hydrocarbon source rock.||||Overlies Stuart Range Formation.||
13151|Mount Toondina Formation|69203|6|Mentioned|p12|Permian|Permian|||||||
13151|Mount Toondina Formation|69454|5|Briefly described|p38:4, 6|Sakmarian|Sakmarian|Arckaringa Basin.||||Lateral equivalent of Purni Formation.||12-JUL-16
13151|Mount Toondina Formation|69554|6|Mentioned|p131|Permian|Permian|Northern Gawler Craton.||||||
13151|Mount Toondina Formation|69673|6|Mentioned|p153 fig 125|||||||Overlies Stuart Range Formation||
13151|Mount Toondina Formation|69946|2|Defined|p2-6, p36, p38, p42, p44-45|Artinskian|Sakmarian|Arckaringa Basin. Townsend and Ludbrook (1975); formerly Mount Toondina beds of Freytag (1965). An 80m type section crops out at Mount Toondina, 45km SSW from Oodnadatta; a subsurface reference section is the interval 187.5 - 516.6m in Cootanoorina 1, showing lower and upper boundaries. Thickness to 598m. Equivalent rocks, named 'Crown Point Formation Unit A' (New, 1988), occur below the Purni Formation in the Pedirka Basin. Early Permian fluviodeltaic sediments.||||Overlies Stuart Range Formation conformably and locally Boorthanna Formation unconformably. Is overlain by Algebuckina Sandstone and  disconformably by Purni Formation.|Basal marine, or marine and lacustrine, grey/dark grey/grey-brown, silty, carbonaceous and micaceous shale; white to grey sandstone and pale grey, friable, clayey siltstone; interbedded sandstone, siltstone, extensive coal and carbonaceous shale.|
13151|Mount Toondina Formation|69948|6|Mentioned|Fig.4.18|||Pedirka Basin.||||Overlies Stuart Range Formation. Is overlain by Purni Formation.||
13151|Mount Toondina Formation|70938|5|Briefly described|p807-808, p815|||Arckaringa Basin.|c.300 Ma.||||Fine to medium clastic detritus.|13-DEC-19
13151|Mount Toondina Formation|71342|3|Fully described|Ch4 p25, Ch5 p2-p5, Ch5 p30|Early Permian|Early Permian|Arckaringa Basin. Deposited in fresh to brackish water lacustrine or a deltal environment. Originally the Mount Toondina beds of Freytag (1965) before being elevated to formation status by Townsend and Ludbrook (1975). A type section at Mount Toondina is given in addition to a subsurface reference section at Cootanoorina 1. This unit is subdivided into three seismically mappable units the lithology of which is described in minor detail. A maximum thickness of 598m is recorded in Boorthanna 1. An equivalent unit in the Pedirka Basin is described in Ch5 p6-p7. See also Ch5 p36, Ch5 p42, Ch5 p44-p45, Ch9 p18, Ch9 p21, Ch11 p6-p7, Ch11 p18.||||Unconformably (in places) overlies the Boorthanna Formation. Conformably overlies the Stuart Range Formation. Unconformably overlain by the Cadna-owie Formation and the Algebuckina Sandstone.|Siltstone and sandstone interbedded with shale and coal.|19-SEP-18
13151|Mount Toondina Formation|72476|6|Mentioned|p36 Fig.9|||Arckaringa Basin. Time-temperature thermal history diagram.||||||
13151|Mount Toondina Formation|72478|5|Briefly described|p6,p8-10, p12, p25-26, p82[doc],|Early Permian|Early Permian|Arckaringa Basin. Shallow marine to lacustrine. Appears as Mt Toondina Formation on p8, Mount Toodina Formation p12, p72-75. See also p51, 70, p82 [of the document].|c. 270-260 Ma|||Conformably overlies the Stuart Range Formation. Unconformably underlies the Algebuckina Sandstone.|Siltstones and sandstones interbedded with coal, shale and rare carbonate units.|29-MAR-21
13151|Mount Toondina Formation|73099|5|Briefly described|Map legend.|Permian.|Late Carboniferous|Arckaringa Basin.||||Overlies Boorthanna Formation. Is overlain conformably by Algebuckina Sandstone and unconformably by Cadna-owie Formation.|Grey claystone and siltstone, carbonaceous in part; grey, clayey and silty very fine- to medium-grained quartz sandstone.|
13151|Mount Toondina Formation|73398|5|Briefly described|p4|||||||Overlies Stuart Range Formation.|Fluvial and lacustrine deposits.|
13167|Mount Victoria Granite|39669|6|Mentioned|Fig.8|||||||||
13167|Mount Victoria Granite|67540|3|Fully described|p25, p27 Tb.1, p28 Tb.2, p38 Fig.2|Calymmian|Calymmian|Named after Mount Victoria, 54 km NW of Manna Hill. Curnamona Province: Olary Domain. Definition reference: this article and Fricke and Hore (2011). High-K, high-Th radiometric signature. Both S-type and I-type granites.|1579-1568 Ma|Of the Crocker Well Suite.||Intrudes Willyama Supergroup.|Massive to weakly foliated, equigranular to locally strongly porphyritic, pink to buff, medium- to coarse-grained, biotite-only or biotite +/- muscovite granites. S-type and I-type granites.|08-FEB-16
13167|Mount Victoria Granite|69562|5|Briefly described|p671 Tb.5|||Magmatic crystalisation age.|1579 +/- 2 Ma (Ludwig and Cooper, 1984).|Unit in Crocker Well Suite.|||Biotite-only to biotite-muscovite granite characterised by large K-feldspar phenocrysts.|06-APR-22
13167|Mount Victoria Granite|69650|2|Defined|p4 Tb.1, p5 Tb.2, p12, p21-24, p29|Calymmian|Calymmian|New name, after Mount Victoria, 54 km NW of Manna Hill. Type locality: Significant outcrop at Mount Victoria, GDA 94, zone 54, 394125 mE, 6463662 mN (Fig. 5) 4 km NE along track from Mt Victoria Hut (GDA 94 389600 mE, 6461600 mN) extends ~5 km SE from edge of outcrop towards Ninnerie Hill. Geochemistry outlined. Generally surrounds Mindamereeka Trondhjemite.|1579-1568 Ma.|Unit in Crocker Well Suite.||Intrudes host Willyama Supergroup metasediments. Is locally intruded by Mindamereeka Trondhjemite.|Massive to weakly foliated, equigranular to locally strongly porphyritic, pink to buff, medium- to coarse-grained biotite-only or biotite+muscovite granites. S-type and I-type.|25-NOV-22
13167|Mount Victoria Granite|70658|5|Briefly described|p33-34, 36|Mesoproterozoic|Mesoproterozoic|Restricted to the Crocker Well region, Plumbago Inlier, Olary Domain, Curnamona Province. Geochemistry very briefly described.|1579-1568 Ma.|Crocker Well Suite.|||Massive to weakly foliated, equigranular to locally strongly porphyritic, pink to buff, medium- to coarse-grained biotite-only or biotite + muscovite granites. S- and I-types.|
13243|Mount Woodroffe Norite|31964|6|Mentioned|p10|||||||||
13243|Mount Woodroffe Norite|31970|4|Described|p14|||?Giles Complex equiv.||||||
13243|Mount Woodroffe Norite|41594|5|Briefly described|p73|||||||||
13247|Mount Wright Volcanics|14019|5|Briefly described|p20|Early Cambrian|Early Cambrian|Geological Province: Gnalta Shelf. Correlative of the Antrim Plateau Volcanics.||||||
13247|Mount Wright Volcanics|22671|3|Fully described|p835,838-39,845-47||Early Cambrian|In the Wonaminta Block.  Mount is Mt in text.||||||11-SEP-07
13247|Mount Wright Volcanics|22857|5|Briefly described|p75, p90 Fig. 14.7B|Early Cambrian|Early Cambrian|Of the Gnalta Group. Basalts and andesites with archaeocyathid limestone lenses. Overlain by Cymbric Vale Formation. Geological Province: Mount Wright Block. See also p94 and p404 App. 1 Tb. A1.4.||||||
13247|Mount Wright Volcanics|22858|5|Briefly described|p75,81,94||Neoproterozoic III|Part of the 'Kara beds' in N.S.W. Max Age: 586 (+/-) 7 Ma.||||||
13247|Mount Wright Volcanics|22859|6|Mentioned|p211|||||||||
13247|Mount Wright Volcanics|23932|5|Briefly described|p665 Table 1|Middle Cambrian|Early Cambrian|||||||
13247|Mount Wright Volcanics|24241|5|Briefly described|p15 Fig.2|Cambrian|Cambrian|Geological Province: Darling Basin.||||||
13247|Mount Wright Volcanics|24263|6|Mentioned|p1385|||Geological Province: Wonominta Block||||||
13247|Mount Wright Volcanics|24509|5|Briefly described|p42|Early Cambrian|Early Cambrian|Mount is Mt in text. Age: ~530-520Ma.||||||
13247|Mount Wright Volcanics|29991|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
13247|Mount Wright Volcanics|30683|6|Mentioned|p45|||||||||
13247|Mount Wright Volcanics|30908|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|Part of Gnalta Group||||||
13247|Mount Wright Volcanics|31705|6|Mentioned|p27|||||||||
13247|Mount Wright Volcanics|32671|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
13247|Mount Wright Volcanics|33000|5|Briefly described|p3|||||||||
13247|Mount Wright Volcanics|33004|6|Mentioned|Fig.8|||||||||
13247|Mount Wright Volcanics|35235|6|Mentioned|p209|||||||||
13247|Mount Wright Volcanics|35320|6|Mentioned|p459|||Structural relationships mentioned||||||
13247|Mount Wright Volcanics|36534|6|Mentioned|p226|||||||||
13247|Mount Wright Volcanics|37461|6|Mentioned|p348|||||||||
13247|Mount Wright Volcanics|38661|6|Mentioned|p7|||||||||
13247|Mount Wright Volcanics|38692|6|Mentioned|Fig.9|||||||||
13247|Mount Wright Volcanics|39214|4|Described|p9|||||||||
13247|Mount Wright Volcanics|39885|6|Mentioned|p431|||See also P433||||||
13247|Mount Wright Volcanics|40455|6|Mentioned|Fig.2|||||||||
13247|Mount Wright Volcanics|40642|6|Mentioned|p163|||||||||
13247|Mount Wright Volcanics|41457|6|Mentioned|p10|||||||||
13247|Mount Wright Volcanics|41810|6|Mentioned|Fig.3|||||||||
13247|Mount Wright Volcanics|42266|6|Mentioned|p299|||||||||
13247|Mount Wright Volcanics|42274|6|Mentioned|p458|||||||||
13247|Mount Wright Volcanics|42910|6|Mentioned|p53|||||||||
13247|Mount Wright Volcanics|42966|5|Briefly described|p299|Cambrian||||||||11-SEP-07
13247|Mount Wright Volcanics|42982|5|Briefly described|p331|||Mount is Mt in text.||||||11-SEP-07
13247|Mount Wright Volcanics|43192|4|Described|p63|Early Cambrian|Early Cambrian|Of Gnalta Group.||||||11-SEP-07
13247|Mount Wright Volcanics|43263|6|Mentioned|Map Legend||Early Cambrian|of Gnaita Group. Spelt Mt.Wright Volcanics.||||||
13247|Mount Wright Volcanics|43502|14|Not recorded|Map Legend||Early Cambrian|(Provisional Edition) Part of Gnalta Group||||||
13247|Mount Wright Volcanics|43560|6|Mentioned|Table 1,p231|||Age: approx. 525 Ma||||||
13247|Mount Wright Volcanics|43704|6|Mentioned|p67|||||||||
13247|Mount Wright Volcanics|44093|5|Briefly described|p108|Cambrian|Cambrian|Underlies Cymbric Vale Volcanics. Medium-K to calc-alkaline volcanics.||||||18-MAR-05
13247|Mount Wright Volcanics|44133|5|Briefly described|p18, 31|Early Cambrian||Geological Province: Wonominta Block. Correlates with Mooracoochie Volcanics.||||||
13247|Mount Wright Volcanics|45102|6|Mentioned|Fig.2|||See also P47||||||
13247|Mount Wright Volcanics|46889|6|Mentioned|p267|||||||||
13247|Mount Wright Volcanics|50327|5|Briefly described|p308|Neoproterozoic|Neoproterozoic|Age: 586Ma (lower section of alkaline rift volcanics). Geological province: Curnamona Craton.  Mount is Mt in text.||||||07-FEB-11
13247|Mount Wright Volcanics|50618|5|Briefly described|p253|Early Cambrian|Early Cambrian|Mount is Mt in text. Geological Province: Wonominta Block.||||||
13247|Mount Wright Volcanics|60567|5|Briefly described|p39, p40|Early Cambrian|Early Cambrian|Calc-alkaline rocks, varying from calc-alkaline andesite to dacite with intrusions of calc-alkaline microdolerite to microdiorite.  Age: 525+/-8Ma (Zhou and Whitford, 1994). Geological Province: Koonenberry Belt.||||||
13247|Mount Wright Volcanics|60990|5|Briefly described|p81-82, p83 Fig.2|Early Cambrian|Early Cambrian|The upper part of this unit contains the same archaeocyath fauna as the overlying Cymbric Vale Formation.||Basal Gnalta Group. ||Underlies the Cymbric Vale Formation conformably.||
13247|Mount Wright Volcanics|62787|5|Briefly described|p77, p81|||Of Gnalta Group. Conformably overlain by Cymbric Vale Formation.||||||14-DEC-15
13247|Mount Wright Volcanics|63489|5|Briefly described|Map legend|Early Cambrian|Early Cambrian|Andesite, basalt, dacite, shale. Mount is Mt in text.||||||
13247|Mount Wright Volcanics|63789|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of Gnalta Group. Mount = Mt in text. Calc-alkaline volcanics: andesite, basalt, dacite, lesser shale and chert, minor limestone with Archaeocyathid fauna.||||||27-NOV-08
13247|Mount Wright Volcanics|63793|5|Briefly described|p22, p34, p62.|Early Cambrian|Early Cambrian|At least 2438 m thick.||Basal unit in Gnalta Group.||Is overlain by Cymbric Vale Formation.|Calc-alkaline basalts and andesites, cherts, limestones and shales.|19-JAN-15
13247|Mount Wright Volcanics|64671|5|Briefly described|Map legend|Early Cambrian|Early Cambrian|Includes calc-alkaline volcanics - andesite, basalt, dacite; shale, minor chert. Mount is Mt in text.||||||26-NOV-08
13247|Mount Wright Volcanics|64679|5|Briefly described|Map legend|Middle Cambrian|Early Cambrian|Of the Gnalta Group. Andesite, basalt and dacite; lesser shale and chert; minor limestone with archaeocyathid fossils.||||||27-NOV-08
13247|Mount Wright Volcanics|64680|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of Gnalta Group. Calc-alkaline volcanics - andesites, basalt, dacite as well as shale and minor chert.||||||01-DEC-08
13247|Mount Wright Volcanics|64684|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of Gnalta Group.||||||
13247|Mount Wright Volcanics|65337|5|Briefly described|p95.|Early Cambrian|Early Cambrian|Gnalta Shelf. Correlative with Kalkarindji Volcanic Group.||Unit in Gnalta Group.||||
13247|Mount Wright Volcanics|65489|6|Mentioned|p119|||||||Correlated with Mooracoochie Volcanics (Warburton Basin).||
13247|Mount Wright Volcanics|66623|3|Fully described|pp57-61, p v, p14. |Early Cambrian|Early Cambrian|Formerly included in lower 'Gnalta Stage' of Mootwingee Series (Kenny 1934); defined as Mount Wright Volcanics by Warris (1967) but published as Mount Wright Formation (Rose and Brunker 1969). Redefined by Crawford et al. (1997) who separated the unit from Mount Arrowsmith Volcanics on basis of geochemistry. Has same calc-alkaline chemistry as felsic tuff in Ponto Group. Abundant archaeocyathids, with algae and sponge spicules, in limestone lenses. 1375 - c.4000m thick. Age-equivalent to Teltawongee and Ponto Groups.||Unit in Gnalta Group.||Faulted against underlying Mount Arrowsmith Volcanics and overlying Cymbric Vale Formation. Faulted on the east against Ravendale Formation.|Calc-alkaline andesite, dacite and minor basaltic andesite intruded by minor calc-alkaline microdolerite to microdiorite dykes; less commonly shale, chert, rare dolomitic limestone lenses.|
13247|Mount Wright Volcanics|66918|5|Briefly described|Map legend|Cambrian|Cambrian|||Unit in Gnalta Group.||Is overlain by Cymbric Vale Formation.|Calc-alkaline volcanics: basalt, andesite and dacite; shaly mudstone, some partly silicified; minor chert beds, limestone with Archaeocyathids, metamorphosed to prehnite-pumpellyite facies; plagioclase-pyroxene dyke or plug weathered to saprolite.|
13247|Mount Wright Volcanics|66927|5|Briefly described|Map legend|Cambrian|Cambrian|Broad areas of long wavelength magnetic features relating to deep sources beneath the Bancannia Trough.|||||Includes andesitic lavas and associated intrusives, minor siltstone, chert and limestone.|
13247|Mount Wright Volcanics|66929|5|Briefly described|Map legend|Early Cambrian|Early Cambrian||||||Calc-alkaline volcanics: andesite, basalt, dacite; shale, minor chert.|
13247|Mount Wright Volcanics|67105|5|Briefly described|p650-653, 655-658, 661, 663, 665|Cambrian|Cambrian|Mount Wright Arc, Koonenberry Belt. Shallow-marine shelf setting; a marginal volcanic arc. Geochemistry discussed in detail.|~511 Ma.|Gnalta Group.||Is overlain by Cymbric Vale Formation. Correlated with the Mooracoochie Volcanics.|A calc-alkaline basalt-andesite-dacite-rhyolite suite, intercalated with a package of mudstone, siltstone and limestone.|
13247|Mount Wright Volcanics|67208|5|Briefly described|Map legend.|Cambrian|Cambrian|||Unit in Gnalta Group.|||Andesitic lavas and associated intrusives, minor siltstone, chert and limestone with archaeocyathid fauna; regionally metamorphosed to prehnite-pumpellyite facies.|
13247|Mount Wright Volcanics|67322|4|Described|p5; Fig.5|Series 2|Series 2|Of Warris (1967); redefined by Crawford et al. (1997). At least 1375m thick: base not exposed. Age determined from fossils, esp. archeocyathans. Occurs in the Mount Wright-Mutawintji region.||Basal unit of the Gnalta Group.||Overlain by the Cymbric Vale Formation: faulted contact.|Calc-alkaline andesite and dacite with minor basaltic andesite, intruded by microdolerite to microdiorite dykes, overlying a lower section of massive dark cherts interbedded with altered basalts, siltstones, and dolomitised limestones.|22-FEB-18
13247|Mount Wright Volcanics|68822|5|Briefly described|p330|Guzhangian|Stage 2|Mount is spelt as Mt in text. Contains a spread of U-Pb SHRIMP ages from 505 +/- 5 Ma, 519 +/- 5 Ma to 521 +/- 5 Ma.||||||
13247|Mount Wright Volcanics|69043|5|Briefly described|p4, p100-101, p104|Early Cambrian|Early Cambrian|Delamerian Orogen. Mount Wright area, eastern side of the Bancannia Trough. Subduction arc related. Source of major magnetic anomalies at depth. Contains archaeocyathid faunas.||||Is overlain by Cymbric Vale Formation.||
13247|Mount Wright Volcanics|69445|5|Briefly described|p30:17|Early Cambrian|Early Cambrian|Gnalta Shelf, western NSW.||Gnalta Group.||Correlated with Kalkarindji Suite.||12-JUL-16
13247|Mount Wright Volcanics|69874|6|Mentioned|p96 Fig .4.1|||Shown as Mt Wright Volcanics in 520 Ma Fig ure.||||||
13247|Mount Wright Volcanics|70013|5|Briefly described|Map legend|Middle Cambrian|Early Cambrian|Koonenberry Belt.||Unit in Gnalta Group.||||
13247|Mount Wright Volcanics|70648|5|Briefly described|Map Legend|Cambrian|Cambrian|Appears to be shown as either partially equivalent to, or including Cymbric Vale Formation.||Gnalta Group|||Andesitic lavas and associated intrusions, minor siltstone, chert and limestone with archaeocyathid fauna.|
13247|Mount Wright Volcanics|70650|5|Briefly described|Map Legend|Cambrian|Cambrian|3 un-named subunits: Mostly shaly mudstone, some partially silicified and minor chert beds: Fine- to medium-grained plagioclase-pyroxene dyke or plug, commonly weathered to a chloritic or montmorillonitic saprolite;  Calc-alkaline volcanics - basalt, andesite and dacite.||Gnalta Group|Includes 3 un-named units.||Andesitic lavas and associated intrusives, minor siltstone, chert and limestone with archaeocyathid fauna.|
13247|Mount Wright Volcanics|70744|5|Briefly described|p945|Middle Cambrian|Early Cambrian|Koonenberry Belt.|||||Quartzose turbidites.|
13247|Mount Wright Volcanics|70838|4|Described|p266-267, p269, p271, p276-278, p280-281|Cambrian|Cambrian|Koonenberry Belt. Deposition by repeated turbidity currents on an E-facing continental slope. Possible tectonic settings discussed. Botomian Stage from fossils.|c.517 Ma.|Gnalta Group.||Is overlain by Cymbric Vale Formation. Is faulted against Grey Range and Mutawintji Groups.|Calc-alkaline volcanics; limestone containing Archaeocyathids in upper part.|
13247|Mount Wright Volcanics|71262|5|Briefly described|p5 Fig 2, p8 Fig 5, p9, p10, 12|Cambrian|Cambrian|May have correlatives under the Bancannia Trough.||Unit of Gnalta Group||||
13247|Mount Wright Volcanics|71593|5|Briefly described|p188-p189|Early Cambrian|Early Cambrian|Koonenberry Province. Interpreted to have been deposited in a continental margin arc. Hosts minor fault related Cu prospects and a barite occurrence.|c. 511-506 Ma|||Overlies the Teltawongee Group.||
13247|Mount Wright Volcanics|72951|6|Mentioned|p1012|Cambrian|Cambrian|Delamarian Orogen. Koonenberry Belt. Described as lower-middle Cambrian.|||||Calc-alkaline volcanics.|
13247|Mount Wright Volcanics|73059|5|Briefly described|p1061|Cambrian|Cambrian|Northwest NSW. Formed in a convergent margin setting: arc to forearc environment. The equivalent deep-marine turbidites are represented by the Teltawongee Group to the NE.|525-505 Ma.|||||
13247|Mount Wright Volcanics|73093|5|Briefly described|map legend|Cambrian|Cambrian||||||Andesite (emplaced as lava), minor meta-siltstone, chert and meta-limestone with Archaeocyathids; mostly shaly mudstone, partly silicified chert beds; Fine- to medium-grained plagioclase-pyroxene saprolitic dyke rock; basalt, andesite and dacite.|09-DEC-21
13247|Mount Wright Volcanics|73177|5|Briefly described|p1098, 1100, 1115 Fig.17|Early Cambrian|Early Cambrian|SHRIMP U-Pb ages by Glen (2013).|521 +/- 5 Ma to 505 +/- 5 Ma.|Gnalta Group.|||Calc-alkaline.|
13247|Mount Wright Volcanics|73430|6|Mentioned|p494, p512|Cambrian|Cambrian|Classified as a volcanic arc suite. [Written as Mt Wright Volcanics.]|508+/-3 Ma, 510-500 Ma||||Calc-alkaline volcanics.|
13289|Moyles Chert Marker Bed|22922|5|Briefly described|33 fig 2|Early Cambrian|Early Cambrian|Of Observatory Hill Formation, Officer basin.||||||
13289|Moyles Chert Marker Bed|23282|2|Defined|p75||Early Cambrian|Age: Early Cambrian 521Ma. of Observatory Hill Formation, Officer Basin. Of Brewer et al (1987).||||||13-MAR-08
13289|Moyles Chert Marker Bed|24112|5|Briefly described|p254 Fig.2|Early Cambrian|Early Cambrian|Of the Marla Group. Geological Province: Officer Basin||||||
13289|Moyles Chert Marker Bed|40945|3|Fully described|p6|Middle Cambrian|Middle Cambrian|||||||
13289|Moyles Chert Marker Bed|43743|6|Mentioned|Fig.2,p33||Early Cambrian|||||||
13289|Moyles Chert Marker Bed|44133|5|Briefly described|p37|Middle Paleozoic|Early Paleozoic|Of the Observatory Hill Formation.||||||07-NOV-08
13289|Moyles Chert Marker Bed|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
13289|Moyles Chert Marker Bed|72478|6|Mentioned|p8|Early Cambrian|Early Cambrian|Officer Basin.||Observatory Hill Formation||||25-MAR-21
13289|Moyles Chert Marker Bed|73099|5|Briefly described|Map legend.|Middle Cambrian|Early Cambrian|Officer Basin.||Observatory Hill Formation.||Is overlain by Oolarinna Member.|Reddish dolostone and siltstone with chert layers, lenses and intraclasts.|
13301|Mud Tank Carbonatite|9199|5|Briefly described|Map legend|||Zircon-apatite-magnetite-ilmenite.  Geological Province: Arunta Block.||||||04-NOV-04
13301|Mud Tank Carbonatite|22524|6|Mentioned|p37|Cryogenian|Cryogenian|||||||
13301|Mud Tank Carbonatite|22804|6|Mentioned|p443|||Geological Province - Arunta Block.  Age - 735+/-5 Ma.||||||
13301|Mud Tank Carbonatite|23844|5|Briefly described|p43|Neoproterozoic|Neoproterozoic|Age: 732 +/- 5Ma (U-Pb zircon, Black and Gulson 1978)||||||
13301|Mud Tank Carbonatite|24047|5|Briefly described|p10|Neoproterozoic|Neoproterozoic|Age: 730Ma.  Geological Province: Arunta province.||||||
13301|Mud Tank Carbonatite|33307|4|Described|p6|||||||||
13301|Mud Tank Carbonatite|35216|6|Mentioned|p51|||||||||
13301|Mud Tank Carbonatite|35521|5|Briefly described|p39|||Chemical analysis.||||||13-NOV-06
13301|Mud Tank Carbonatite|38885|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
13301|Mud Tank Carbonatite|39213|3|Fully described|p6|||||||||
13301|Mud Tank Carbonatite|39552|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
13301|Mud Tank Carbonatite|39583|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
13301|Mud Tank Carbonatite|39610|4|Described|p14|||See also p7.||||||13-NOV-06
13301|Mud Tank Carbonatite|39621|3|Fully described|p12|||||||||
13301|Mud Tank Carbonatite|39887|6|Mentioned|Fig.3|||||||||
13301|Mud Tank Carbonatite|39888|6|Mentioned|Table 1|||||||||
13301|Mud Tank Carbonatite|40811|4|Described|p320|||||||||
13301|Mud Tank Carbonatite|41509|6|Mentioned|p4|||||||||
13301|Mud Tank Carbonatite|41830|6|Mentioned|p549|||||||||
13301|Mud Tank Carbonatite|42481|6|Mentioned|Fig.1 P183|||||||||
13301|Mud Tank Carbonatite|46830|6|Mentioned|p23|||||||||
13301|Mud Tank Carbonatite|46868|6|Mentioned|p79|||||||||
13301|Mud Tank Carbonatite|46884|4|Described|p227|||||||||
13301|Mud Tank Carbonatite|48992|2|Defined|p38|Neoproterozoic|Neoproterozoic|||||||
13301|Mud Tank Carbonatite|49444|14|Not recorded|?|||||||||
13301|Mud Tank Carbonatite|50246|5|Briefly described|p6, p7, p19 Fig. 1|||Name also presented as the informal Mud Tank carbonatite. Age: 732+/-5Ma. Potassic alkaline igneous suite that hosts orthomagmatic PGE-Au-Cu-Ni deposits. Also referred to as the Mud Tank carbonatite complex.||||||07-FEB-11
13301|Mud Tank Carbonatite|60525|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Geological Province: Arunta Block. Carbonatite, eluvium containing magnetite, apatite and zircon.||||||
13301|Mud Tank Carbonatite|60547|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Internediate to ultrabasic. Zircon-apatite-magnetite-illmenite-phlogopite carbonatite.||||||
13301|Mud Tank Carbonatite|65341|6|Mentioned|p2 Fig.2. |||||||||
13301|Mud Tank Carbonatite|66860|6|Mentioned|p2 fig 2|||||||||
13301|Mud Tank Carbonatite|67127|6|Mentioned|p98, p100, p107, p109, p172|Neoproterozoic|Neoproterozoic|Located near the Woolanga Lineament in a zone that also features the Nolans Bore deposit; however it should be noted a recent date for the host veins of 1244 +/- 10 Ma (Korsch et al, 2009; U-Pb) suggests the mineralisation is not related to this unit. 52km north-northwest of the Mordor Complex.|732 +/- 5 Ma (U-Pb; Black and Gulson, 1978)||||Features significantly higher Cu, Ni and Cr contents and lower Sr, Zr, Nb, Mo, La and Ce contents than average carbonatites. Occurs near the Woolanga Lineament.|
13301|Mud Tank Carbonatite|69418|6|Mentioned|p3:31, 34|||Arunta Region. Hosts gem quality garnet, zircon and apatite at Gemtree (Harts Range area), and vermiculite at Mud Tank (described).||||||12-JUL-16
13301|Mud Tank Carbonatite|69427|4|Described|p12:40 Fig.12.34; 12:46, 64|Neoproterozoic|Neoproterozoic|Shaw et al. (1979), Crohn and Moore (1984), Currie et al. (1992). Near the N margin of the Strangways Range, Aileron Province. Deformed carbonatite with steeply-dipping to subvertical foliation/layering. Vermiculite has been mined since 1996, with reserves providing a mine life of ~20 years; fossicking for coarse zircons occurs. Age by TIMS conventional U-Pb method on zircon separates.|732 +/- 5 Ma (Black and Gulson, 1978).|||Intrudes Yambah Granulite.|Crystalline carbonate rocks; foliated micaceous carbonate rocks, rich in pale brown phlogopite; feldspathic carbonate rocks with variable amounts of sodic plagioclase, clinopyroxene, amphibole and biotite. Significant vermiculite occurs.|12-JUL-16
13301|Mud Tank Carbonatite|69585|6|Mentioned|p6-7|||Mentioned as a standard for zircon dating.||||||
13301|Mud Tank Carbonatite|69729|5|Briefly described|p66, p85|Neoproterozoic|Neoproterozoic|Black and Gulson (1978). Underlies Amadeus Basin. Less formally presented as the Mud Tank carbonatite complex on p85.|c.732 Ma.|||||
13301|Mud Tank Carbonatite|69929|6|Mentioned|p243|||NW Gough Dam Shear Zone, Arunta Block. Has well-foliated margins, and gradational contacts with enveloping pelitic schists and mylonites.|732 +/- 5 Ma (U-Pb; Black and Gulson, 1978).|||||
13301|Mud Tank Carbonatite|70789|5|Briefly described|p320|||Apatite from this unit was used as an in-house secondary standard for LA-ICP-MS.||||||
13301|Mud Tank Carbonatite|70825|6|Mentioned|p41|||||||||
13301|Mud Tank Carbonatite|71858|6|Mentioned|p69|||Aileron Province.|ca. 732 Ma|||||
13323|Mudnawatana Tonalite|22631|6|Mentioned|p176|Paleozoic|Paleozoic|Age: 427+/- 133 Ma.||||||07-NOV-08
13323|Mudnawatana Tonalite|23478|5|Briefly described|p28|Silurian|Ordovician|Age: 427+/-133 Ma||||||
13323|Mudnawatana Tonalite|23804|6|Mentioned|p18|||||||||
13323|Mudnawatana Tonalite|35397|4|Described|p97|||Petrography. Previously known as Mudnawanta Granite.||||||
13323|Mudnawatana Tonalite|40642|6|Mentioned|p173|||||||||
13323|Mudnawatana Tonalite|42624|6|Mentioned|p24|Ordovician|Cambrian|Cambrian-Ordovician||||||22-APR-10
13323|Mudnawatana Tonalite|43052|5|Briefly described|p56 Table 7.3, p55|||Of Mount Babage Inlier.||||||11-NOV-13
13323|Mudnawatana Tonalite|44133|5|Briefly described|p55, 56 Table 7.3|Ordovician|Ordovician|Geological Province: Mount Babbage Inlier. Oligoclase-microline-biotite tonalite. I-Type. Age: 427 +/- 133Ma.||||||
13323|Mudnawatana Tonalite|62962|5|Briefly described|p2283 Fig. 1(c), p2285, p2284 Fig. 2|Paleozoic|Paleozoic|Geological Province: Mount Babbage Inlier, Mount Painter Province. Suggest a I-type.||||||07-FEB-11
13323|Mudnawatana Tonalite|67536|5|Briefly described|Map Legend|Sakmarian|Katian|Kanmantoo Province; basement to Murray Basin.|ca. 442 +/- 6 Ma - 427 +/- 133 Ma||||Late/post-Delamerian felsic intrusive rocks.|
13323|Mudnawatana Tonalite|68068|5|Briefly described|Map legend|Silurian|Silurian|Formerly the Mudnawatana Granite. Delamerian syn- to post-tectonic granitoid.|427 +/- 133 Ma (Rb-Sr).||||Medium-grained, equigranular, white to grey granodiorite to tonalite, locally with xenoliths and associated coarse-grained felsic pegmatite dykes and apophyses.|11-NOV-13
13323|Mudnawatana Tonalite|68713|6|Mentioned|p19, p22|||Restricted to the Mount Babbage Inlier. Associated pegmatite dykes are weakly deformed.||||||
13323|Mudnawatana Tonalite|69019|4|Described|p23, p27-29 Figs.7-9, p70-71, p145.|Ordovician|Cambrian|Of Teale (1979); formerly Mudnawatana Granite (Bowes, 1953); Coats and Blissett (1971) included it and other intrusions in their Younger Granite Suite. Geochemistry decribed. Dating problems discussed briefly.|c.440 Ma.|||Intrudes Wattleowie and Terrapinna Granites, Radium Creek Group.|Equigranular pale grey to pale pinkish grey, fine- to medium-grained tonalite; reddish-yellow weathering colours; weak foliation.|
13323|Mudnawatana Tonalite|69023|4|Described|p24-27, p37, p42, p50-51, p74-77|Ordovician|Cambrian|See also p147, p189. Originally Mudnawatana Granite of Bowes (1953); later extended to include similar intrusions (in the Mount Painter Inlier) in the Younger Granite Suite of Coats and Blissett (1971); Teale (1979) revised the nomenclature and reclassified the unit as Mudnawatana Tonalite, restricted again to the Mount Babbage Inlier. Geochemistry detailed.|427 +/- 133 Ma Rb-Sr (Teale and Mortimer, 1995).|||Intrudes all phases of Moolawatana Suite.|An equigranular grey granitoid with reddish-yellow weathering colours; weak foliation; recrystallisation of most mineral phases is evident; numerous undeformed very coarse-grained felsic leuco-pegmatite dykes. I-type.|
13323|Mudnawatana Tonalite|70384|5|Briefly described|Map legend.|Silurian|Ordovician|Age is of either time of metamorphism or emplacement.|431 +/- 7 Ma (Rb-Sr whole rock + biotite).|||Probable correlative of Gordon Springs Granodiorite.|White to grey, medium-grained, equigranular granodiorite to tonalite +/- local enclaves or associated coarse-grained felsic pegmatite apophyses.|
13323|Mudnawatana Tonalite|72456|5|Briefly described|Map Legend|Ordovician|Cambrian|Marree 1:250k map sheet.  Related to an unnamed pegmatite.|427 +/- 133 Ma||||Tonalite, weakly foliated, medium-grained granitoid of quartz, feldspars and biotite.|
13323|Mudnawatana Tonalite|72459|6|Mentioned|p67|Delamerian|Mesoproterozoic|Originally defined by Teale (1979). Together with the Paralana granodiorite, the Gordon Springs Granodiorite and the British Empire Granite forms so called group 3 of this study. Chemically very similar to the Gordon Springs Granodiorite and the Paralana granodiorite and on that basis group these 3 units together into the Paralana granodiorite.|||||Granodioritic and granitic components.|
13323|Mudnawatana Tonalite|75063|6|Mentioned|p94 Fig.2|||Northern Flinders Ranges area.||||||
13402|Muloowurtie Formation|23768|5|Briefly described|p28 Fig.5, p123|Late Eocene|Late Eocene|Geological Province: St Vincent Basin.||||||29-MAR-05
13402|Muloowurtie Formation|30251|6|Mentioned|p3|||Refs Stuart (1970)||||||
13402|Muloowurtie Formation|33330|1|Redefined|p154|late Eocene|late Eocene|||||||
13402|Muloowurtie Formation|35689|6|Mentioned|Fig.33|||Stratigraphic correlation, St.Vincent Basin.||||||
13402|Muloowurtie Formation|36119|6|Mentioned|p52|||||||||
13402|Muloowurtie Formation|38699|6|Mentioned|p12|||||||||
13402|Muloowurtie Formation|41513|6|Mentioned|p43|||See also P45||||||
13402|Muloowurtie Formation|41626|6|Mentioned|p50|||||||||
13402|Muloowurtie Formation|43667|6|Mentioned|Fig.3,p12||Eocene|||||||
13402|Muloowurtie Formation|44133|5|Briefly described|p164, 165 Fig. 10.11|Late Eocene|Middle Eocene|Correlative of the Clinton Formation. Includes the Quartoo Sand Member.||||||
13402|Muloowurtie Formation|60958|5|Briefly described|Map Legend|Eocene|Eocene|Calcareous siltstone or silty calcarenite, cross-bedded sandstone and basal conglomerate. Geological Province: Saint Vincent Basin.||||||
13402|Muloowurtie Formation|61121|5|Briefly described|Map legend|Eocene|Eocene|Includes the Quartoo Sand Member. Calcareous siltstone or silty calcarenite, cross-bedded sandstone and basal conglomerate; contains foraminfera 'Fibularia gregata', echinoids and crinoids. Geological Province: St. Vincent Basin.||||||06-JUN-05
13402|Muloowurtie Formation|65375|4|Described|p34, pp49-50.|Late Eocene|Late Eocene|Named by Stuart (1970); formerly the Muloowurtie Clays of Tepper (1879). Type section at Sliding Rocks. Thickness to 67m. Represents fluvial-shoreface and marginal marine deposits of Late Eocene age. Divided into two parts by Quartoo Sand Member. Deposited in Tertiary graben to half-graben structure in Wallaroo Group-Arthurton Granite basement.|||Includes Quartoo Sand Member.|Unconformably overlies Kulpara Formation. Is overlain unconformably by Rogue Formation.|A succession of calcareous siltstone or silty limestone, rich in foaraminifers, echinoids, crinoids and other fossil groups; cross-bedded fluvial sandstone and conglomerate in the lower part.|
13402|Muloowurtie Formation|65891|6|Mentioned|p221 Fig.5. |Paleogene|Paleogene|Western St Vincent Basin. Bartonian to Priabonian age.||||||
13402|Muloowurtie Formation|67462|5|Briefly described|Map legend.||Eocene|Western Saint Vincent Basin.|||Includes Quartoo Sand Member.|Is overlain by Throoka Silt.||
13402|Muloowurtie Formation|68715|6|Mentioned|p31 Fig.5|Bartonian|Lutetian|St Vincent Basin.||||||
13402|Muloowurtie Formation|70382|5|Briefly described|p28, p29 Fig 3, p30|Eocene|Eocene|Geological province: St Vincent Basin. Fossils include foraminifera, echinoids and crinoids.|||Includes the Quartoo Sand Member.||Basal conglomerate overlain by cross-bedded sandstone and calcareous and glauconitic quartz sands. Sand: variously glauconitic, calcareous, fossiliferous; silt; conglomerate.|
13405|Mumbalo Pedoderm|31532|3|Fully described|Table 1|||||||||
13430|Mundi Mundi Granite|22771|6|Mentioned|p42,49||Mesoproterozoic|||||||
13430|Mundi Mundi Granite|22857|6|Mentioned|p49|Mesoproterozoic|Mesoproterozoic|||||||
13430|Mundi Mundi Granite|23818|5|Briefly described|p35|Calymmian|Calymmian|Of the Willyama Complex. Age: 1520 Ma. Geological Province: Willyama Block.||||||
13430|Mundi Mundi Granite|29863|6|Mentioned|p350|||||||||
13430|Mundi Mundi Granite|29864|6|Mentioned|Fig.1|||||||||
13430|Mundi Mundi Granite|29865|6|Mentioned|Fig.1|||||||||
13430|Mundi Mundi Granite|29991|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
13430|Mundi Mundi Granite|30177|6|Mentioned|p195|||1560 Ma||||||26-FEB-13
13430|Mundi Mundi Granite|30260|6|Mentioned|Fig.2|||||||||
13430|Mundi Mundi Granite|30908|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
13430|Mundi Mundi Granite|31012|6|Mentioned|p8|||Lithology. Carpentarian||||||
13430|Mundi Mundi Granite|31435|6|Mentioned|p38|||||||||
13430|Mundi Mundi Granite|31595|6|Mentioned|Table 1|||||||||
13430|Mundi Mundi Granite|31596|6|Mentioned|p282|||||||||
13430|Mundi Mundi Granite|32671|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
13430|Mundi Mundi Granite|33004|6|Mentioned|p126|||||||||
13430|Mundi Mundi Granite|33287|6|Mentioned|Fig.1|||||||||
13430|Mundi Mundi Granite|33472|6|Mentioned|p475|||||||||
13430|Mundi Mundi Granite|33875|6|Mentioned|p17|||Uranium mineralisation.||||||
13430|Mundi Mundi Granite|34469|6|Mentioned|p109|||Upper Proterozoic. See also pp110,111||||||26-FEB-13
13430|Mundi Mundi Granite|34534|6|Mentioned|Fig.2.12|||||||||
13430|Mundi Mundi Granite|34537|6|Mentioned|p35|||1520my||||||
13430|Mundi Mundi Granite|34550|6|Mentioned|p23|||||||||
13430|Mundi Mundi Granite|34604|6|Mentioned|p251|||K/Ar age||||||
13430|Mundi Mundi Granite|34812|6|Mentioned|p12|||||||||
13430|Mundi Mundi Granite|34834|6|Mentioned|p219|||||||||
13430|Mundi Mundi Granite|34896|6|Mentioned|p296|||||||||
13430|Mundi Mundi Granite|35199|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
13430|Mundi Mundi Granite|36584|6|Mentioned|Fig.19-42|||||||||
13430|Mundi Mundi Granite|37581|6|Mentioned|p76|||||||||
13430|Mundi Mundi Granite|37931|6|Mentioned|p534|||||||||
13430|Mundi Mundi Granite|38068|6|Mentioned|p67|||||||||
13430|Mundi Mundi Granite|38411|6|Mentioned|Fig.2|||||||||
13430|Mundi Mundi Granite|39214|6|Mentioned|p5|||||||||
13430|Mundi Mundi Granite|39638|6|Mentioned|Table 1|||||||||
13430|Mundi Mundi Granite|39640|6|Mentioned|p208|||||||||
13430|Mundi Mundi Granite|39652|6|Mentioned|p4|||||||||
13430|Mundi Mundi Granite|39885|6|Mentioned|Fig.1|||||||||
13430|Mundi Mundi Granite|40291|6|Mentioned|Fig.3|||||||||
13430|Mundi Mundi Granite|40582|5|Briefly described|p467|||||||||
13430|Mundi Mundi Granite|41402|6|Mentioned|p37|||||||||
13430|Mundi Mundi Granite|41405|5|Briefly described|p204|||||||||
13430|Mundi Mundi Granite|42090|6|Mentioned|p18|||||||||
13430|Mundi Mundi Granite|42813|6|Mentioned|p13|||||||||
13430|Mundi Mundi Granite|43052|6|Mentioned|p92|||||||||
13430|Mundi Mundi Granite|43269|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
13430|Mundi Mundi Granite|43344|14|Not recorded|p2|||Intrudes Willyama Complex||||||
13430|Mundi Mundi Granite|43491|14|Not recorded|pI/37|||||||||
13430|Mundi Mundi Granite|43501|14|Not recorded|Map Legend|Neoproterozoic|Mesoproterozoic|(Provisional Edition)||||||
13430|Mundi Mundi Granite|43502|14|Not recorded|Map Legend||Mesoproterozoic|(Provisional Edition)  1307-1466 my. Radiometric age||||||
13430|Mundi Mundi Granite|45003|14|Not recorded|p30|||||||||
13430|Mundi Mundi Granite|46595|14|Not recorded|p.283-287,301-307|||On many pages. p.310,311,313,319.  Age determinations. 1820 +/- 100 m.y. (H54-15,I54-3).||||||
13430|Mundi Mundi Granite|46597|14|Not recorded|p186|||||||||
13430|Mundi Mundi Granite|46889|6|Mentioned|p276|||||||||
13430|Mundi Mundi Granite|48894|6|Mentioned|p9|||Age. See also pp10,11.||||||26-FEB-13
13430|Mundi Mundi Granite|50081|5|Briefly described|p43|Calymmian|Calymmian|Age: ~1590 Ma. Geological Province: Curnamona Province.||||||24-FEB-05
13430|Mundi Mundi Granite|50606|5|Briefly described|p5.15|||Geological Province: Broken Hill Block.||||||
13430|Mundi Mundi Granite|50619|5|Briefly described|p175|Mesoproterozoic|Mesoproterozoic|Age: ca 1.59Ga.  Geological Province: Broken Hill Block.||||||12-AUG-04
13430|Mundi Mundi Granite|60485|5|Briefly described|p28 Fig. 2|||Age: 1600-1580Ma.  Geological Province: Broken Hill Domain.||||||03-MAR-05
13430|Mundi Mundi Granite|60657|5|Briefly described|p13 Fig. 2|Mesoproterozoic|Mesoproterozoic|Age: ~1500Ma. Geological Province: Curnamona Craton.||||||10-MAY-05
13430|Mundi Mundi Granite|62592|5|Briefly described|p16 Fig.2.2. |Calymmian|Statherian|Broken Hill Domain, Curnamona Province.|c.1600 - 1580 Ma.|||||
13430|Mundi Mundi Granite|63020|5|Briefly described|p987 Fig. 8|Mesoproterozoic|Mesoproterozoic|Age: 1590Ma. Geological Province: Curnamona Province (Broken Hill Domain).||||||10-AUG-07
13430|Mundi Mundi Granite|63102|5|Briefly described|p13,51|||Geological province: Broken Hill Domain, Curnamona Province.|~1600-1580 Ma|||||
13430|Mundi Mundi Granite|63489|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Geological Province: Mount Babbage Inlier.||||||10-SEP-07
13430|Mundi Mundi Granite|63866|6|Mentioned|p37-p38, p49||||1591 +/- 5 Ma (Page et al., 2005a)|||||
13430|Mundi Mundi Granite|64743|6|Mentioned|p344 Fig.5. |||Intruded the Broken Hill Block during the Olarian Orogeny. Age is U/Pb SHRIMP age from Page et al. 2005.|1591 +/- 5 Ma.|||||04-JUN-15
13430|Mundi Mundi Granite|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Broken Hill Domain.|1591 +/- 5 Ma.|||||
13430|Mundi Mundi Granite|68126|5|Briefly described|p5-6|||Broken Hill Domain, Curnanoma Province. Occurs in Cusin Creek pluton and Brewery Creek pluton. Appears as Mundi Mundi granite on p6. Three age determinations (Page, 2006; Page et al., 2000) are in the age range c.1580 - c.1596 Ma.|||||Non-foliated, leucocratic 2-mica granite.|
13430|Mundi Mundi Granite|70657|5|Briefly described|p13 Fig.6, p48, p56|Calymmian|Statherian|Curnamona Province, Broken Hill Domain. Associated with Willyama Supergroup. Syn- to post-tectonic granites. Appears as Mundi Mundi Granites in Fig.6.|~1600-1580 Ma.|Ninnerie Supersuite.|||Granites.|
13430|Mundi Mundi Granite|71968|6|Mentioned|p5|||Geological province: Curnamona province.||||||
13430|Mundi Mundi Granite|72461|6|Mentioned|p6|||Gawler Craton. Broken Hill Domain.|1591 +/- 5 Ma|||||
13430|Mundi Mundi Granite|72949|6|Mentioned|p36|Calymmian|Calymmian|Curnamona Province. Broken Hill / Olary Blocks. See also Mundi Granite p35.|1591 +/- 5 Ma|||||24-DEC-21
13536|Murray Bridge Granite|9124|5|Briefly described|Map Legend|Paleozoic|Paleozoic|Pink, coarse-grained, granite.||||||07-NOV-08
13536|Murray Bridge Granite|23023|6|Mentioned|p1799||Arenig|Max Age: 471 (+/-) 12 Ma.||||||
13536|Murray Bridge Granite|23869|5|Briefly described|p15 Fig. 3|Ordovician|Ordovician|||||||
13536|Murray Bridge Granite|30758|5|Briefly described|p67|||Genesis, magmatic intrusion||||||
13536|Murray Bridge Granite|32432|4|Described|Table 1|||See also Fig.2||||||
13536|Murray Bridge Granite|32433|6|Mentioned|p80|||See also Table 2||||||
13536|Murray Bridge Granite|33490|6|Mentioned|p11|||Delamerian. c.470my||||||
13536|Murray Bridge Granite|40499|6|Mentioned|p148|||||||||
13536|Murray Bridge Granite|42154|5|Briefly described|p335|||||||||
13536|Murray Bridge Granite|42222|6|Mentioned|p26|||||||||
13536|Murray Bridge Granite|42271|5|Briefly described|p384|||||||||
13536|Murray Bridge Granite|42275|6|Mentioned|Table 2 P474|||||||||
13536|Murray Bridge Granite|42761|5|Briefly described|Fig.1 P6|||||||||
13536|Murray Bridge Granite|44133|5|Briefly described|p51 Fig. 7.18, 56 Table 7.3|Ordovician|Ordovician|A-Type. Massive coarse grained granite. Age: 471 +/- 12Ma.||||||
13536|Murray Bridge Granite|45003|14|Not recorded|p42|||||||||
13536|Murray Bridge Granite|61525|5|Briefly described|p40|||Also referred to as the "Swanport Granite"||||||
13536|Murray Bridge Granite|64769|6|Mentioned|p28|Plaeoproterozoic|Paleoproterozoic|Dimension stone name.||||||06-MAY-09
13536|Murray Bridge Granite|67536|5|Briefly described|Map Legend|Darriwilian|Stage 3|Kanmantoo Province; basement to Murray Basin.|ca. 497 +/- 10 Ma - 471 +/- 12 Ma||||Late/post-Delamerian felsic intrusive rocks.|
13536|Murray Bridge Granite|71322|5|Briefly described|p52 Fig.1|Ordovician|Cambrian|Late/post Delamerian.|497+/-10 Ma - 471+/-2 Ma.||||Felsic intrusive rocks.|
13536|Murray Bridge Granite|73093|5|Briefly described|map legend|Ordovician|Cambrian||||||Granite, massive, coarse-grained. A-type.|09-DEC-21
13544|Murray Group|2967|5|Briefly described|p15 Fig.2.2, p24|Miocene|Oligocene|Ludbrook (1957). His Ettrick Formation was added to the Group as Ettrick Marl by Lawrence (1966). Western Murray Basin. Late Oligocene to middle Miocene.|||Geera Clay, Ettrick Marl, Duddo Limestone, Winnambool Formation, Bookpurnong beds, Parilla Sand.|Overlies Renmark Group. Is interbedded with Wunghnu Group.|Marine sequence.|
13544|Murray Group|10010|5|Briefly described|p12 Fig. 3|Middle Miocene|Early Oligocene|Includes Ettrick Formation, Mannum, Duddo and Gambier Limestones, and Winnabool Formation. Geological Province: Murray Basin.||||||13-AUG-07
13544|Murray Group|22587|6|Mentioned|p79 Fig.7|Middle Miocene|Late Oligocene|||||||
13544|Murray Group|22773|5|Briefly described|p351|Middle Miocene|Early Oligocene|||||||
13544|Murray Group|22799|3|Fully described|p29|||||||||
13544|Murray Group|22857|5|Briefly described|p351, p352 Fig.24.8|Middle Miocene|Early Oligocene|Marine to marginal marine deposits. Geological Province: Murray Basin.||||||
13544|Murray Group|22887|5|Briefly described|Fig.6 p13, p33|Middle Miocene|Late Oligocene|||||||
13544|Murray Group|23226|5|Briefly described|p890|||Originally included Mannum Formation, Finniss Clay, Morgan Limestone (including Caddell Marl lens) and Pata Limestone (Ludbrook 1961). Superseded by Murray Supergroup.||||||10-SEP-19
13544|Murray Group|23230|4|Described|Table4-1p40, 42, 44|Miocene|Oligocene|||||||
13544|Murray Group|23768|5|Briefly described|p33-34|||Raised to supergroup status by Lukasik and James (1998). Geological Province: Murray Basin.||||||
13544|Murray Group|23884|5|Briefly described|p153, p155 Gif. 13.2|Middle Miocene|Late Oligocene|Geological Province: Murray Basin.||||||
13544|Murray Group|24096|6|Mentioned|p4|||Geological Province: Murray Basin.||||||
13544|Murray Group|24106|5|Briefly described|p184|Miocene|Miocene|Geological Province: Murray Basin.||||||
13544|Murray Group|24361|6|Mentioned|p50, Fig.1b|||||||||
13544|Murray Group|24551|6|Mentioned|p322 Fig. 10.29, 543|||||||||
13544|Murray Group|24563|5|Briefly described|p485|Middle Miocene|Late Oligocene|Proposed by Lukasik and James(1998) to be raised to supergroup status.  Now reinstated as Murray Group.  Geological Province: Murray Basin.||||||
13544|Murray Group|29355|6|Mentioned|p179|||||||||
13544|Murray Group|31170|6|Mentioned|p295|||Aquifer systems||||||
13544|Murray Group|31625|6|Mentioned|Fig. 5.2|||Oligocene-Miocene||||||
13544|Murray Group|31746|3|Fully described|p194|||||||||
13544|Murray Group|31848|6|Mentioned|p12|||Refers Ludbrook (1961)||||||
13544|Murray Group|31849|6|Mentioned|p7|||||||||
13544|Murray Group|34308|6|Mentioned|p182|||||||||
13544|Murray Group|34418|6|Mentioned|p506|||See also P507||||||
13544|Murray Group|34735|5|Briefly described|p32|||||||||
13544|Murray Group|35187|6|Mentioned|Table1|||||||||
13544|Murray Group|36305|6|Mentioned|p358|||||||||
13544|Murray Group|37873|6|Mentioned|p1|||||||||
13544|Murray Group|38601|6|Mentioned|p5|||||||||
13544|Murray Group|40003|6|Mentioned|p38|||||||||
13544|Murray Group|41511|5|Briefly described|p18|||||||||
13544|Murray Group|41868|6|Mentioned|p551|||||||||
13544|Murray Group|42125|5|Briefly described|p135|||See also Fig.5||||||
13544|Murray Group|42126|6|Mentioned|p159|||||||||
13544|Murray Group|42127|5|Briefly described|p218|||See also Fig.1||||||
13544|Murray Group|42128|5|Briefly described|p227|||See also Fig.2||||||
13544|Murray Group|42129|6|Mentioned|p254|||See also Fig.6||||||
13544|Murray Group|42130|6|Mentioned|p264|||See also Fig.2||||||
13544|Murray Group|42133|6|Mentioned|p307|||||||||
13544|Murray Group|42134|6|Mentioned|Fig.3 P335|||||||||
13544|Murray Group|42137|5|Briefly described|p367|||See also Fig.2||||||
13544|Murray Group|42138|6|Mentioned|p388|||||||||
13544|Murray Group|42184|6|Mentioned|Fig.2 P348|||||||||
13544|Murray Group|42623|5|Briefly described|p2|||limestone, aquifer||||||
13544|Murray Group|42720|5|Briefly described|map legend|Miocene|Oligocene|||||||
13544|Murray Group|42813|6|Mentioned|p24|||||||||
13544|Murray Group|42827|4|Described|p268|||||||||
13544|Murray Group|42881|4|Described|Fig.3, P84|||||||||
13544|Murray Group|42966|3|Fully described|p113, 124|||||||||
13544|Murray Group|43195|5|Briefly described|Map Legend|Miocene|Oligocene|See also commentary on back of map.||||||
13544|Murray Group|43218|4|Described|Fig.3,p22||Middle Miocene|||||||
13544|Murray Group|43780|6|Mentioned|p5|||||||||
13544|Murray Group|43791|6|Mentioned|p372, Fig1|||||||||
13544|Murray Group|43801|6|Mentioned|p114|||||||||
13544|Murray Group|43804|6|Mentioned|p47|||||||||
13544|Murray Group|44133|5|Briefly described|p158|Middle Miocene|Late Oligocene|||||||
13544|Murray Group|44191|5|Briefly described|Map Legend|Middle Miocene|Early Oligocene|||||||
13544|Murray Group|45168|6|Mentioned|Table 1|||||||||
13544|Murray Group|49038|5|Briefly described|p26|||||||||
13544|Murray Group|49040|6|Mentioned|p11|||||||||
13544|Murray Group|50154|2|Defined|p26, p133, p135|Miocene|Oligocene|Geological Province: Murray Basin. Overlies the Renmark Group.||||||15-SEP-04
13544|Murray Group|50155|5|Briefly described|Map Legend|Miocene|Oligocene|Includes Ettrick Marl and Duddo Limestone||||||
13544|Murray Group|50156|5|Briefly described|Map Legend|Miocene|Oligocene|Includes the Ettrick Marl and Duddo Limestone.||||||
13544|Murray Group|50157|5|Briefly described|Map Legend|Miocene|Oligocene|Includes: Ettrick Marl, Duddo Limestone||||||
13544|Murray Group|50158|5|Briefly described|Map Legend|Miocene|Oligocene|Includes: Ettrick Marl, Duddo Limestone||||||
13544|Murray Group|50159|5|Briefly described|Map Legend|Miocene|Oligocene|Includes: Ettrick Marl, Duddo Limestone||||||
13544|Murray Group|50160|5|Briefly described|Map Legend|Miocene|Oligocene|Includes: Ettrick Marl, Duddo Limestone||||||
13544|Murray Group|50161|5|Briefly described|Map Legend|Miocene|Oligocene|Includes: Ettrick Marl, Duddo Limestone||||||22-JUN-04
13544|Murray Group|50162|5|Briefly described|Map Legend|Miocene|Oligocene|Includes the Ettrick Marl and Duddo Limestone.||||||22-JUN-04
13544|Murray Group|50163|5|Briefly described|Map Legend|Miocene|Oligocene|Includes: Ettrick Marl, Duddo Limestone||||||24-JUN-04
13544|Murray Group|50164|5|Briefly described|Map Legend|Miocene|Oligocene|Includes: Ettrick Marl, Duddo Limestone||||||
13544|Murray Group|60421|5|Briefly described|p409|Miocene|Oligocene|Includes: Duddo Limestone||||||
13544|Murray Group|60451|5|Briefly described|p95 Fig. 61|||||||||
13544|Murray Group|60452|5|Briefly described|p15|Tertiary|Tertiary|Geogical Province: Murray Basin.||||||
13544|Murray Group|60461|5|Briefly described|Map legend|Pliocene|Oligocene|Includes the Shepparton and Calivil Formations.||||||
13544|Murray Group|60491|5|Briefly described|p16|Pliocene|Late Oligocene|||||||
13544|Murray Group|60538|6|Mentioned|p473 Fig.12|||||||||
13544|Murray Group|60540|5|Briefly described|p1000 Fig.2|Miocene|Miocene|Of Firman (1972), Rogers et al. (1995). Replaced by Murray Supergroup in this paper.||||||06-FEB-18
13544|Murray Group|60599|6|Mentioned|p15|Middle Miocene||Geological Province: Murray Basin.||||||
13544|Murray Group|61155|5|Briefly described|p4, p18|Middle Miocene|Late Oligocene|Shallow-marine calcarenites consisting of skeletal debris and quartz sand. Geological Province: Murray Basin.||||||
13544|Murray Group|61185|5|Briefly described|p58, p15|||Marine sediments. Geological Province: Murray Basin.||||||07-FEB-11
13544|Murray Group|61314|5|Briefly described|p129|Miocene|Oligocene|Geological Province: Murray Basin.||||||
13544|Murray Group|61837|5|Briefly described|p217|||Includes the Compton Conglomerate. Geological Province: Murray Basin.||||||
13544|Murray Group|61841|5|Briefly described|p242, p244|Miocene|Oligocene|Carbonate-dominated sediments. Geological Province: Murray Basin.||||||
13544|Murray Group|62370|6|Mentioned|p453|||Geological Province: Murray Basin.||||||
13544|Murray Group|63066|5|Briefly described|p485-486|||Nomenclature (preferred by P.A. Rogers over Murray Supergroup) consistent with that used for sediment packages of similar magnitude in the Murray Basin: Renmark Group, Heytesbury Group and Eucla Group.||||||22-MAY-13
13544|Murray Group|63887|5|Briefly described|p20, p21 Fig. 1|Middle Miocene|Late Early Oligocene|Includes; Geera Clay, Ettrick and Winnambool Formations and Mannum Limestone. Lagoonal and marginal marine muddy facies and in deeper waters, marl and limestone.||||||
13544|Murray Group|64237|4|Described|p17-20|Middle Miocene|Late Oligocene|Detailed nomenclatural history is presented in this paper, commencing with the Ludbrook stratigraphic scheme through to the controversial upgrade of the Murray Group to Murray Supergroup followed by the reinstatement of the Murray Group.||||||18-SEP-09
13544|Murray Group|64569|6|Mentioned|p893|||||||||
13544|Murray Group|64961|5|Briefly described|p259|Miocene|Miocene|Geological province: Murray Basin.||||||21-APR-09
13544|Murray Group|65552|4|Described|p5 Fig. 3, p6, p26 App.5|Middle Miocene|Late Oligocene|Western Murray Basin. Deposited during a marine incursion. Contemporaneous with Geera Clay and Winnambool, Ettrick and Olney Formations to the east. Contains Mannum Formation and Pata, Morgan, Duddo, and Gambier Limestones.||||||
13544|Murray Group|65687|6|Mentioned|p189|Late Miocene|Oligocene|Parent of Morgan Limestone.||||||
13544|Murray Group|65715|6|Mentioned|p11 Tb.7|||Paleogene? Miocene?||||||
13544|Murray Group|65969|5|Briefly described|p27 Tb.3.3|Miocene|Oligocene|Includes Calivil Formation.||||||
13544|Murray Group|66002|5|Briefly described|p10 Tb.7|Paleogene|Paleogene|Includes Duddo Limestone. Defined by Ludbrook 1957.||||||
13544|Murray Group|66286|5|Briefly described|p179.|Miocene|Oligocene|Southern Murray Basin.|||Includes Duddo Limestone.||Dominated by shallow-marine platform limestones deposited during a marine transgression-regression into the Basin.|
13544|Murray Group|66287|6|Mentioned|p33|Miocene|Miocene||||||Limestones.|20-APR-12
13544|Murray Group|67061|6|Mentioned|p554 Fig.10.|Miocene||Murray Basin.||||||
13544|Murray Group|67462|5|Briefly described|Map legend.|Miocene|Miocene|Murray Basin.|||Includes Mannum Limestone, Winnambool Formation and Geera Clay.|||
13544|Murray Group|68140|5|Briefly described|p1701-1704, p1707|||See also Murray Group Limestone. Up to 130m thick. Enveloped by the Ettrick Formation, Geera Clay, Bookpurnong Beds, and Winnambool Formation.||||Underlain by the Renmark Formation. Overlain by the Loxton-Parilla Sands.|Comprises marine and marginal marine limestone with calcareous sands, marls, and silts.|09-FEB-18
13544|Murray Group|68189|6|Mentioned|p27 Tb.3.2, p29||||||Includes the Winnambool Formation, Geera Clay, and Duddo Limestone.|||
13544|Murray Group|68194|5|Briefly described|p22|||Murray Basin.|||Includes Geera Clay and Calivil Formation.|Overlies Renmark Group.||
13544|Murray Group|68715|5|Briefly described|p31 Fig.5|Miocene|Miocene|Murray Basin. Early to Middle Miocene age.|||Includes Cadell, Finniss, Mannum, Ettrick and Winnambool Formations; Geera Clay.|||07-APR-17
13544|Murray Group|69562|6|Mentioned|p674|||||||||
13544|Murray Group|70718|6|Mentioned|p25, p103||||||Includes the Geera Clay, Winnambool Formation. .||Limestones.|30-MAY-19
13544|Murray Group|71593|5|Briefly described|p51, p54|||Murray Basin.|||Includes the Duddo Limestone, Winnambool Formation, Ettrick Formation and the Geera Clay.|Overlies the Renmark Group. Overlain by the Wunghu Group.||
13544|Murray Group|72445|5|Briefly described|App.1, App2; App.5; App.7 p4-5, p7, p20.|Miocene|Oligiocene|App.2 is a .csv format file. Identified in Stavely 05,07,08,11,12, 14,16. Said (App.7 p7) to include Gambier, Duddo, Morgan and Patta Limestone Members in the far west of the basin; Geera Clay in the centre of the basin.|||Includes Calivil Formation, Geera Clay, Bookpurnong Formation, Ettrick Formation, Gambier Limestone, Duddo Limestone, Morgan Limestone, Winnambool Formation and Pata Limestone|Overlies Renmark Group (sharp  or gradational contact) and underlies Wunghnu Group (sharp or gradational contact), Bookpurnong Formation (sharp contact).|Glauconitic marl and limestone and light to dark grey micaceous and pyritic muddy sand and sand. Muddy sand and lesser carbonate and marl at base.|
13544|Murray Group|73118|5|Briefly described|p12, 82-83|Miocene|Oligocene|Murray Basin. Has large reserves of groundwater. Mainly concealed, but forms cliffs of River Murray gorge. Shallow-marine platform deposits.|||Winnambool, Ettrick, Mannum Formations; Geera, Finniss Clays; Gambier, Morgan, Pata, Duddo Limestones; Cadell Marl; Compton Conglomerate.||Includes skeletal calcarenite, calcareous-cemented quartz sandstone, marl, and bioclastic and micritic limestones. Characterised by abundant fragmental skeletal debris of diverse fossil assemblages.|
13544|Murray Group|73228|4|Described|p50, p52-57, p59-60|Early Oligocene|Late Early Oligocene|Murray Basin. [An informal lower subdivision is mentioned but not explicitly as a distinct unit]. Deposited on a shallow marine platform and includes lagoonal, marginal marine to estuarine, and shallow marine carbonate platform depositional environments. Identified in Cooltong 1, Berri North 1, Nadda 1, Loxton 1, and Overland Corner 1 drillholes.|||Cadell Formation, Finniss Formation, Geera Clay, Ettrick Formation, Winnambool Formation, Mannum Formation.|Underlain by Gambier Limestone, Ettrick Formation, and Renmark Group. Overlain by Bookpurnong Formation.|Shallow marine fossiliferous limestone and sandstone with minor clay and silt.|02-NOV-22
13544|Murray Group|73229|5|Briefly described|p66-67, p70-72, p74-75|Middle Miocene|Mid Oligocene|Murray Basin. [Analysed using pXRF; see article]. [An informal lower subdivision is frequently mentioned but not explicetly as a distinct unit].|||Cadell Formation, Finniss Formation, Geera Clay, Winnambool Formation, Mannum Formation, Ettrick Formation||Includes limestone, echinoidal, bryzoal, crinoidal; sandstone, calcareous; minor carbonaceous clay and silt.|
13544|Murray Group|73505|5|Briefly described|p2, p11, p13, p36|Miocene|Oligocene|Murray Basin. Generally thickens to the west.|||Geera Clay, Calivil Group|Overlies Olney Formation, Mologa Surface|Varies from 40-160 m thick.|
13577|Murta Formation|13497|5|Briefly described|p115, p115 fig 6.33, p130, p138|Early Cretaceous|Early Cretaceous|Eromanga Basin, Dullingari Field. Deposited in a high-sinuosity fluvial, overbank, lacustrine or proximal deltal environment. This formation is an oil source rock. Oil and gas reservoir. See also p138 fig 8.17, p141, p142, p146, p151 fig 9.23, p152 fig 9.26, p170, p171, p183, p188, p216.|||Includes the McKinlay Member.|Overlies the Namur Sandstone. Overlain by the Cadna-owie Formation.|Sandstones, siltstone, shale and minor coal.|
13577|Murta Formation|13516|6|Mentioned|p167 fig 10, p171 fig 12|Early Cretaceous|Early Cretaceous|In Eromanga Basin.||||||
13577|Murta Formation|22839|6|Mentioned|P33|||||||||
13577|Murta Formation|22883|5|Briefly described|P31, Fig2||Early Cretaceous|Overlain by Cadna-owie Formation, underlain by Namur Sandstone.||||||17-JAN-08
13577|Murta Formation|22912|5|Briefly described|33|||Geological Province: Eromagna Basin.||||||17-JAN-08
13577|Murta Formation|23054|6|Mentioned|Fig5p22|Valanginian|Berriasian|||||||
13577|Murta Formation|23154|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|Geological Province - Eromanga Basin.  Includes McKinlay Member.||||||
13577|Murta Formation|23155|3|Fully described|p28 & Fig 15 on p28|Early Cretaceous|Early Cretaceous|The Murta Formation is Early Cretaceous (Neocomian) in age, from spore pollen determination.  See p28 for details of type section etc.||||||
13577|Murta Formation|23356|5|Briefly described|26 Tab.2|Neocomian|Neocomian|||||||
13577|Murta Formation|23375|4|Described|Fig2 p265|Valanginian|Berriasian|Laterally equivalent to upper Hooray Sandstone. In the Eromanga Basin.||||||17-JAN-08
13577|Murta Formation|23982|5|Briefly described|p58 Fig.18|||Geological Province: Eromanga Basin.||||||
13577|Murta Formation|24092|5|Briefly described|p8 Fig.3|||Geological Province: Eromanga Basin.||||||
13577|Murta Formation|24210|5|Briefly described|p133 Fig. 2|Early Cretaceous|Early Cretaceous|Includes the McKinlay Member.  Geological Province: Eromanga Basin.||||||
13577|Murta Formation|24372|6|Mentioned|p22|||Geological Province: Cooper Basin.||||||
13577|Murta Formation|24482|5|Briefly described|p44|Cretaceous|Jurassic|Contains the McKinlay Member. Geological Province: Eromanga Basin.||||||
13577|Murta Formation|37287|6|Mentioned|p36|||||||||
13577|Murta Formation|41705|6|Mentioned|p128|||||||||
13577|Murta Formation|42071|6|Mentioned|p117|||||||||
13577|Murta Formation|44133|4|Described|p111, 104 Fig. 9.11|Neocomian|Neocomian|Geological Province: Eromanga Basin. Formerly upper part of the Mooga Formation known as the Murta Member. Overlies and intertongues with McKinlay Member and Namur Sandstone. Overlain transitionally by Cadna-owie Formation.||||||08-MAY-13
13577|Murta Formation|60717|5|Briefly described|p40 Fig. 2, p42|Early Cretaceous|Late Jurassic|Contains the McKinlay member. Overlies Westbourne Formation; overlain by Cadna-owie Formation; interfingers partially with Algebuckina Sandstone. Geological Province: Eromanga  Basin.||||||31-JAN-08
13577|Murta Formation|61614|5|Briefly described|p289, p294, p295, p290 Fig. 2|Early Cretaceous|Early Cretaceous|Geological Province: Eromanga Basin. Largely carbonaceous siltstones deposited in lacustrine and paralic environments.||||||17-MAR-09
13577|Murta Formation|61615|6|Mentioned|p302 Fig. 2|Early Cretaceous|Late Jurassic|Geological Province: Eromanga Basin.||||||07-FEB-11
13577|Murta Formation|62028|6|Mentioned|p11|||May provide a regional seal.||||||26-FEB-08
13577|Murta Formation|62029|5|Briefly described|p15 Fig. 4|||See also Murta Member.||||||08-APR-08
13577|Murta Formation|62537|6|Mentioned|p191 Fig.2, p192.|Early Cretaceous|Early Cretaceous|Eromanga Basin. Significant hydrocarbon source potential.||||Overlies Birkhead Formation. Is overlain by Cadna-owie Formation.||
13577|Murta Formation|63979|2|Defined|p44, Fig. 44|Valanginian|Berriasian|Supersedes "Murta Member" in SA; also now extended to Qld. Passes laterally into upper part of Hooray Sst. Prev. referred to as Murta Member of Mooga Formation by petroleum companies.Detailed desc./explans. lithology/nomenclature included||||Laterally equivalent to upper part of Hooray Sandstone.||09-APR-13
13577|Murta Formation|64048|5|Briefly described|p64 Tb. 2, p70|||Geological Province: Eromanga Basin. Possesses relatively low hydrocarbon source potential.||||||07-FEB-11
13577|Murta Formation|64665|5|Briefly described|p53 Fig.2, p62.|Early Cretaceous|Early Cretaceous|Eromanga Basin.||||Overlies Namur Sandstone. Is overlain by Cadna-owie Formation.||
13577|Murta Formation|65385|5|Briefly described|pS134 Fig.7|Early Cretaceous|Early Cretaceous|Of Eromanga Basin. Overlies Namur Sandstone. Overlain by Cadna-owie Formation.||||||08-MAR-12
13577|Murta Formation|65489|5|Briefly described|p15, p47, p49, p55, p73, p96, p132, p152|Early Cretaceous|Early Cretaceous|See also p154-158, p160. Eromanga Basin. 60m thick. Hydrocarbon source rock. Oil reservoir accounting for 10% of the Basin's production. Intraformational shale regional seal.|||Includes McKinlay Member.|Overlies Namur Sandstone. Is overlain by Cadna-owie Formation.|Lacustrine turbidite sandstones.|
13577|Murta Formation|65925|5|Briefly described|Appendix 2.||||||||Dark grey, argillaceous and carbonaceous siltstone with interbedded fine- to very fine-grained sandstone.|
13577|Murta Formation|66529|6|Mentioned|p12 Fig.5|||Eromanga Basin.||||Overlies Namur Sandstone. Is overlain by Cadna-owie Formation.||
13577|Murta Formation|66623|5|Briefly described|pp240-242.|||Not identified in outcrop for this study, although recognised in borehole sections. Largely non-marine.|||||Interbedded siltstone, shale, very fine-grained sandstone and minor medium- to coarse-grained sandstone.|
13577|Murta Formation|66915|5|Briefly described|p6 Fig.3|Early Cretaceous|Early Cretaceous|Eromanga Basin.||||||
13577|Murta Formation|67561|5|Briefly described|p52 Fig.2|Valanginian|Berriasian|Australian Spore-Pollen zonation: australiensis.||||||
13577|Murta Formation|68068|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Eromanga Basin. Subsurface only.|||Includes McKinlay Member at base.|Overlies Namur Sandstone. Is overlain conformably by Parabarana Sandstone and Cadna-owie Formation.|Dark grey laminated carbonaceous siltstone, graded beds, ripple marks with interbeds of fine-grained to locally coarse-grained sandstone, ripple laminated, bioturbated; carbonate cemented layers near top; diagenetic siderite common.|
13577|Murta Formation|68731|6|Mentioned|pp209-211|||||||||
13577|Murta Formation|69001|6|Mentioned|p16|Early Cretaceous|Jurassic|Recent interpretations by the NSW DPI broadly group this unit within the Algebuckina Sandstone and equivalent units.||||||
13577|Murta Formation|69019|5|Briefly described|p85 Fig.21.|Valanginian|Berriasian|Southern Eromanga Basin.|||Includes McKinlay Member.|Overlies Namur Sandstone. Is overlain by Cadna-owie Formation.||
13577|Murta Formation|69023|4|Described|p79, p86, p89 Fig.20, p92, p191-192|Valanginian|Berriasian|Defined by Nugent (1969) as Murta Member, part of the Mooga Formation; later elevated to Formation status (Callen et al.,1994; Gravestock et al., 1995) and the Mooga Formation was discarded. The McKinlay Member (Mount, 1982) became a Member of the Murta Formation. Eromanga Basin. Thickness from ~33 to >53m. Stratigraphic wells intersection data.|||Includes McKinlay Member.|Overlies Namur and Algebuckina Sandstones. Passes laterally into Algebuckina Sandstone. Is overlain gradationally by Cadna-owie Formation.|Dark grey argillaceous and carbonaceous siltstone interbedded with fine- to very fine-grained sandstone, diagenetic siderite and calcite nodules and layers; overlain by thinly interbedded siltstone and sandstone; passing up into dark grey siltstone.|
13577|Murta Formation|69454|6|Mentioned|p38:13|||The uppermost shale of previous usage (eg Ambrose and Heugh, 2010) was referred to basal Cadna-owie Formation by Gray et al. (2002). This Formation, with the underlying Namur Sandstone (in the Cooper Basin), are equivalent to the upper Algebuckina Sandstone in the Poolowanna Trough.||||||12-JUL-16
13577|Murta Formation|69457|5|Briefly described|p41:3-5, 7|Early Cretaceous|Early Cretaceous|Eromanga Basin.||||Overlies Namur Sandstone. Is overlain conformably by Cadna-owie Formation.||12-JUL-16
13577|Murta Formation|69594|5|Briefly described|p519, p526-528, p531-532, p573|Hauterivian|Berriasian|Eromanga Basin; mostly in SA. Generally 50-60m thick; possibly >100m locally. Brackish environment. A significant hydrocarbon reservoir; has hydrocarbon source potential.||||Overlies Namur Sandstone; conformably overlies upper Namur Sandstone. Is overlain conformably/transitionally by Cadna-owie Formation. Lateral equivalent of (upper) Hooray Sandstone.|Interbedded and interlaminated sublabile to quartzose sandstone, silty sandstone, siltstone and lesser mudstone, intraformational conglomerate and coal.|
13577|Murta Formation|69673|6|Mentioned|p154, p155 fig 127|Cretaceous|Cretaceous|||||Overlies Namur Sandstone, overlain by Cadna-owie Formation||
13577|Murta Formation|69790|6|Mentioned|p1063 Fig.2|Cretaceous|Cretaceous|Eromanga Basin.||||||
13577|Murta Formation|69797|5|Briefly described|p17 incl Fig.2|Early Cretaceous|Early Cretaceous|The best petroleum source rocks in Jurassic-Cretaceous sequence of Eromanga Basin are organic-rich shales and siltstones of the Murta Formation, the coals and carbonaceous shales of Birkhead Formation, and highly carbonaceous shales of Poolowanna Formation. Geol. Prov: Eromanga Basin.||||||17-JAN-17
13577|Murta Formation|69946|2|Defined|p11, p17-19, p56-58, p86-92|Early Cretaceous|Early Cretaceous|Siltstone and shale in the upper part of the Mooga Formation were defined as Murta Member by Nugent (1969); raised to Formation status by Gravestock et al. (1995). Equivalent to the upper Hooray Sandstone in Qld. Type section is the interval 1469.14 - 1526.13m in Dullingari North 1. Up to >90m thick. Wireline log correlations. Sedimentary facies log.|||Includes McKinlay Member.|Overlies and intertongues with Namur Sandstone. Is overlain gradationally by Cadna-owie Formation. Intertongues with Algebuckina Sandstone.|Thinly interbedded dark grey siltstone, shale, pale grey very fine- to fine-grained sandstone; minor medium- and coarse-grained sandstone. Diagenetic siderite nodules and layers.|
13577|Murta Formation|69947|5|Briefly described|p3, p8, p13 Fig.7.2, p29-31 Figs.7.18-20|Early Cretaceous|Early Cretaceous|Eromanga Basin. Widespread meandering fluvial, floodplain and lacustrine facies. Represents two major transgressive-regressive cycles; illustrated by a well log from the Maxwell Field.|||McKinlay Member.|Conformably overlies Namur, Hooray Sandstones. Is overlain conformably by Cadna-owie Formation.|Sandstone, siltstone.|
13577|Murta Formation|69948|6|Mentioned|Fig.4.2|||Eromanga Basin (an intracratonic basin). Sediment thickness, sonic log, gamma ray log all shown in contrast with Otway Basin (a rift basin).||||Overlies Namur Sandstone. Is overlain by Cadna-owie Formation.||
13577|Murta Formation|70821|5|Briefly described|p31|||Previously part of the [obsolete] "Lower Hooray Sandstone". 44 m thick interval, between 395 and 439 m in Weilmoringle 1 well. See also Murta Member p21||||Overlies Namur Sandstone.||02-DEC-16
13577|Murta Formation|70823|4|Described|p25-p27, p43-p44, p78|Early Cretaceous|Early Cretaceous|Eromanga Basin. Up to 60m thick. Deposited in a meandering-anastomosing fluvial or lacustrine or overbank environments.|||Includes the McKinlay Member.|Overlies the Namur Sandstone. Overlain by the Cadna-owie Formation.|Sandstone, siltstone, shale and coal.|
13577|Murta Formation|70824|5|Briefly described|p9|Cretaceous|Jurassic|Eromanga Basin.||||Overlies the Westbourne Formation. Overlain by the Cadna-owie Formation.||
13577|Murta Formation|71321|6|Mentioned|p15|||Of Eromanga Basin.||||Overlies the Algebuckina Sandstone, Namur Sandstone and the McKinlay Member.||24-OCT-19
13577|Murta Formation|71342|6|Mentioned|Ch 1 p6, Ch 1 p19, Ch4 p9, Ch5 p12|Cenomanian|Berriasian|Originally defined by Nugent (1969) as siltstone and shale in the upper part of the Mooga Formation. Gravestock et al, (1995) elevated the name to Murta Formation. This unit is equivalent to the upper Hooray Sandstone in Queensland. The type section is in Dullingari North 1 (Mount, 1981). Diagenetic siderite nodules and layers produce distinctive spikes on sonic and density logs. This unit has a maximum thickness >90m in the Nappamerri Trough. Age based partly on palynology. Interpreted to have been deposited in open lacustrine, lacustrine fan delta, distributary channel and lacustrine shoreline environments. A brackish to marine environment is suggested for the upper parts of this formation. Spore-pollen zone is given in Ch5 p57. A complete sedimentary facies log is given in Ch5 p88. Source rock characteristics are described in detail in Ch8 (p6). Forms a seal over the Namur Sandstone. Oil is produced from a very thin by extensive, high-permeability shoreface sand. See also  Ch5 p17-p18, Ch5 p30, Ch5 p32, Ch5 p57-p58, Ch5 p85-p92, Ch6 p5, Ch6 p7, Ch7 p3, Ch7 p8, Ch7 p11, Ch7 p13, Ch7 p29-p31, Ch8 p2, Ch8 p5-p6, Ch8 p8, Ch8 p10, Ch8 p17, Ch8 p22, Ch10 p3, Ch10 tbl 10.1, Ch10 p8, Ch10 p14, Ch10 p17-p20, Ch11 p2-p5, Ch11 p7-p8, Ch11 p17, Ch12 p5, Ch13 p2-p3, Ch13 p7, Ch13 p9-p10, Ch13 p25-p28, Ch13 p31, Ch13 p33, Ch14 p5.|||Includes the McKinlay Member.|Intertongues with and overlies the McKinlay Member and the Namur Sandstone. Conformably overlain by the Cadna-owie Formation. Intertongues with and is equivalent to the Algebuckina Sandstone.|Thinly interbedded dark grey siltstone, shale, pale grey, very fine to fine-grained sandstone and minor medium and coarse-grained sandstone.|
13577|Murta Formation|71863|6|Mentioned|p5|Hauterivian|Berriasian|Eromanga Basin.||||Overlies Namur Sandstone, overlain by Cadna-owie Formation.||
13577|Murta Formation|72297|5|Briefly described|p739, p742-743|||Eromanga Basin. Petroleum reservoir, with marginal source rock potential. Oil flows >2000 bpd in Dullingari North 1 (in SA).||||||
13577|Murta Formation|72298|5|Briefly described|p801|Cretaceous|Cretaceous|Eromanga Basin (SA,QLD). Main confined aquifers, generally producing flowing artesian water bores.|||McKinlay Member.|Overlies Namur Sandstone. Is overlain by Cadna-owie FZ.||
13577|Murta Formation|73251|6|Mentioned|p55-56, p62|Early Cretaceous|Early Cretaceous|Eromanga Basin. Deposited in freshwater lacustrine conditions. Capable of generating hydrocarbons (marginally mature for liquid hydrocarbon generation); constitutes the most shallow-lying and demonstrably effective petroleum source within the stacked Warburton, Cooper, and Eromanga Basins. Partly self-sourcing and likely to have contributed to hydrocarbon accumulations within the overlying Namur Sandstone and Cadnaowie Formation. Depositional environments included lacustrine turbidites, deltas, and shoreface.||||Underlain by and equivalent to Namur Sandstone. Overlain by [and equivalent to?] Cadna-owie Formation.||
13577|Murta Formation|73281|6|Mentioned|Appendix (DIP)|||See DIP034_Petroleumdata.xlsx and DIP034_Welldata.xlsx.||||||
13586|Murteree Shale|13497|3|Fully described|iv, v, xi, p58, p69 fig 6.1|Kungurian|Artinskian|Cooper Basin. Defined by Gatehouse (1972), name is derived from Lake Murteree. Originally included in the Moomba Formation before Gatehouse raised it to formation status. A type section from core is mentioned. Is relatively uniform in thickness with a maximum thickness of 80m in the Nappamerri Trough. Interpreted to have been deposited in a broad, fresh-water lake. This unit forms an important regional seal over the Patchawarra Formation. Wireline log results are discussed. See also p70, p89, p93-p97, p101-p102, p117, p129, p131, p132, p150-p151, p160, p163, p170-p175.||Gidgealpa Group||Conformably overlies and intertongues with the Patchawarra Formation. Conformably overlain by the Epsilon Formation. Unconformably overlain by the Toolachee Formation.|Black to dark grey-brown argillaceous siltstone and fine-grained sandstone. Fine-grained pyrite and muscovite are charateristic and carbonaceous siltstone also occurs.|
13586|Murteree Shale|13516|6|Mentioned|p147, fig 5|Early Permian|Early Permian|From Cooper Basin||||||
13586|Murteree Shale|22839|6|Mentioned|P33|||||||||
13586|Murteree Shale|22883|6|Mentioned|P29|||||||||
13586|Murteree Shale|23154|5|Briefly described|Map Legend|Early Permian|Early Permian|Geological Province - Cooper Basin.  Parent - Gidgealpa Group.||||||
13586|Murteree Shale|23155|4|Described|p19|Early Permian|Early Permian|Spore and pollen indicate an Early Permian age. The unit is wide spread on STRZELECKI and relatively uniform in thickness (50+/- 25m).||||||
13586|Murteree Shale|23340|6|Mentioned|12|||||||||
13586|Murteree Shale|23375|4|Described|Fig2 p265,285||Artinskian|In the Cooper Basin.||||||17-JAN-08
13586|Murteree Shale|23832|4|Described|p329|Permian|Permian|Of Gidgealpa Group. Geological Province: Cooper Basin.||||||
13586|Murteree Shale|24199|5|Briefly described|p512 Fig.2|Early Permian|Early Permian|Geological Province: Cooper Basin.||||||
13586|Murteree Shale|24210|5|Briefly described|p133 Fig. 2|Permian|Permian|Of the Gidgealpa Group.  Overlies the Patchawarra Formations; underlies the Epsilon Formation.  Geological Province: Cooper Basin.  See also p132.||||||
13586|Murteree Shale|29387|6|Mentioned|Table 2|||Refers to Gatehouse 1972.||||||
13586|Murteree Shale|29391|6|Mentioned|Table 5|||See p23.||||||
13586|Murteree Shale|29721|6|Mentioned|p137|||||||||
13586|Murteree Shale|30540|6|Mentioned|Fig.6|||||||||
13586|Murteree Shale|30544|6|Mentioned|p53|||Map legend||||||
13586|Murteree Shale|30825|6|Mentioned|p37|||||||||
13586|Murteree Shale|30873|2|Defined|p14|Permian|Permian|Part of Gidgealpa Group.||||||17-JAN-08
13586|Murteree Shale|30921|6|Mentioned|Map legend|Artinskian|Sakmarian|Sakmarian - Artinskian||||||
13586|Murteree Shale|32696|6|Mentioned|Fig.4|||See also Figs 6 & 7||||||
13586|Murteree Shale|33074|6|Mentioned|p260|||||||||
13586|Murteree Shale|33331|6|Mentioned|p42|||||||||
13586|Murteree Shale|33489|6|Mentioned|Fig.2|||Refers Kapel (1972) & Gatehouse (1972)||||||
13586|Murteree Shale|33976|6|Mentioned|Fig.5|||||||||
13586|Murteree Shale|34839|6|Mentioned|Fig.2|||||||||
13586|Murteree Shale|35067|6|Mentioned|Fig.4|||||||||
13586|Murteree Shale|35068|6|Mentioned|Fig.3|||Discussed P58.||||||
13586|Murteree Shale|35279|6|Mentioned|Fig.5|||||||||
13586|Murteree Shale|35457|6|Mentioned|Fig.4|||Biostratigraphic relationships||||||
13586|Murteree Shale|35573|6|Mentioned|Fig.7|||Generalised stratigraphy - Southern Cooper Basin||||||
13586|Murteree Shale|35845|4|Described|p23|||Lithology and depositional environments. See also p62.||||||17-JAN-08
13586|Murteree Shale|36099|6|Mentioned|Fig.2|||||||||
13586|Murteree Shale|36910|6|Mentioned|p62|||||||||
13586|Murteree Shale|36917|6|Mentioned|Fig.1|||||||||
13586|Murteree Shale|37855|6|Mentioned|Fig.2|||||||||
13586|Murteree Shale|37917|6|Mentioned|Fig.2|||||||||
13586|Murteree Shale|38977|6|Mentioned|p1423|||||||||
13586|Murteree Shale|39252|5|Briefly described|p20|||||||||
13586|Murteree Shale|39254|5|Briefly described|p46|||||||||
13586|Murteree Shale|39261|6|Mentioned|Fig. 9|||||||||
13586|Murteree Shale|39264|6|Mentioned|Fig. 13|||||||||
13586|Murteree Shale|39276|6|Mentioned|Fig. 2|||||||||
13586|Murteree Shale|39445|5|Briefly described|Table 8|||||||||
13586|Murteree Shale|39478|6|Mentioned|Table 1|||||||||
13586|Murteree Shale|39494|6|Mentioned|Fig.3|||||||||
13586|Murteree Shale|40030|6|Mentioned|Fig.3|||||||||
13586|Murteree Shale|40249|6|Mentioned|p45|||||||||
13586|Murteree Shale|40544|6|Mentioned|Fig.4|||||||||
13586|Murteree Shale|41060|6|Mentioned|Fig.5|||||||||
13586|Murteree Shale|41099|6|Mentioned|p190|||||||||
13586|Murteree Shale|41131|5|Briefly described|Table 1|||||||||
13586|Murteree Shale|41164|6|Mentioned|Table 1|||||||||
13586|Murteree Shale|41183|6|Mentioned|Fig.3 p308|||||||||
13586|Murteree Shale|41189|6|Mentioned|p260|||||||||
13586|Murteree Shale|41198|6|Mentioned|Table 1|||||||||
13586|Murteree Shale|41214|6|Mentioned|Fig.3|||||||||
13586|Murteree Shale|41247|6|Mentioned|Fig.5|||||||||
13586|Murteree Shale|41267|6|Mentioned|Fig.2|||||||||
13586|Murteree Shale|41288|6|Mentioned|p158|||||||||
13586|Murteree Shale|41290|6|Mentioned|Fig.8|||||||||
13586|Murteree Shale|41595|6|Mentioned|p31|||||||||
13586|Murteree Shale|41720|6|Mentioned|p373|||||||||
13586|Murteree Shale|42085|6|Mentioned|Fig.2 P374|||||||||
13586|Murteree Shale|42395|5|Briefly described|Fig.13 P83|||||||||
13586|Murteree Shale|42746|5|Briefly described|p6|||||||||
13586|Murteree Shale|42999|5|Briefly described|Table 2,p90||Early Permian|||||||
13586|Murteree Shale|43002|5|Briefly described|Fig.2,p135|||||||||
13586|Murteree Shale|43018|5|Briefly described|Table 1,p386|||||||||
13586|Murteree Shale|43105|5|Briefly described|p14|||||||||
13586|Murteree Shale|43570|5|Briefly described|Fig.2,p535,544|Kungurian|Artinskian|||||||
13586|Murteree Shale|43628|6|Mentioned|Fig.3||Early Permian|||||||
13586|Murteree Shale|44133|4|Described|p65 Fig. 8.3, 84|Kungurian|Artinskian|Of the Gidgealpa Group. Geological Province: Cooper Basin. Conformably overlies: Patchawarra Formation. Up to 80m thick. Conformably underlies: Epsilon Formation.||||||
13586|Murteree Shale|46849|6|Mentioned|Fig. 7|||||||||
13586|Murteree Shale|60386|6|Mentioned|p296|Artinskian|Artinskian|Cooper Basin. Non-marine.||||||
13586|Murteree Shale|60717|5|Briefly described|p40 Fig. 2|Kungurian|Artinskian|Of Gidgealpa Group. Overlies Patchawarra Formation; underlies Epsilon Formation. Thickness: 80m. Geological Province: Cooper Basin.||||||31-JAN-08
13586|Murteree Shale|61614|6|Mentioned|p290 Fig. 2|Early Permian|Early Permian|Of Gidgealpa Group. Geological Province: Cooper Basin.||||||17-MAR-09
13586|Murteree Shale|61615|5|Briefly described|p302, p302 Fig. 2|Early Permian|Early Permian|Of Gidgealpa Group. Conformbaly underlain by Parchawarra Formation. Geological Province: Cooper Basin.||||||07-FEB-11
13586|Murteree Shale|61616|6|Mentioned|p330 Fig. 2|Early Permian|Early Permian|Of Gidgealpa Group. Geological Province: Cooper Basin.||||||
13586|Murteree Shale|62046|5|Briefly described|p125 Fig. 2|Permian|Permian|Geological Province: Cooper-Eromanga Basins.||||||14-APR-08
13586|Murteree Shale|62537|6|Mentioned|p191 Fig.2. |Early Permian|Early Permian|Cooper Basin.||Unit in Gidgealpa Group.||Overlies Patchawarra Formation. Is overlain by Epsilon Formation.||
13586|Murteree Shale|63832|6|Mentioned|p131 fig 2|Cisuralian|Cisuralian|Of Cooper Basin.||||||14-MAR-14
13586|Murteree Shale|63978|2|Defined|p13, Fig. 3|Early Permian|Early Permian|Originally interp. by Kapel (1972) as lower third of Moonbi Fm. Conformably overlies Patchawarra Fm; conformably underlies Epsilon Fm. Dark grey-brown to black, laminated, argillaceous siltstone + lesser fine-gr.sandstone (more lith. incl.). Thick: 80m.||||||07-FEB-11
13586|Murteree Shale|64048|5|Briefly described|p63, p64 Tb. 2|||Geological Province: Cooper Basin. Acts as the seal for Patchawarra Formation reservoirs.||||||07-FEB-11
13586|Murteree Shale|64197|6|Mentioned|p625 Fig.1c, p630 Fig.7|Middle Permian|Middle Permian|Cooper Basin.||||Overlies the Patchawarra Formation; underlies the Epsilon Formation.||11-DEC-15
13586|Murteree Shale|64631|5|Briefly described|p44 Fig.2.|Kungurian|Artinskian|Cooper Basin. Biostratigraphic age control for base and top.||||Overlies Patchawarra Sandstone. Showns as overlain by Roseneath/Epsilon.||
13586|Murteree Shale|64665|5|Briefly described|p53 Fig.2.|Early Permian|Early Permian|Cooper Basin.||||Overlies Patchawarra Formation. Is overlain by Epsilon Formation.||
13586|Murteree Shale|65489|5|Briefly described|p45-46, p48-49, p96, p131-132, p143|Kungurian|Artinskian|Cooper Basin. 80m thick. Relatively little hydrocarbon source potential. Seal for Patchawarra Formation.||Unit in Gidgealpa Group.||Overlies Patchawarra Formation. Is overlain by Epsilon Formation and Roseneath Shale.|Lacustrine shale unit.|
13586|Murteree Shale|65925|5|Briefly described|Appendix 2.||||||||Siltstone, grey-green, shaly, with thin lenses of fine-grained sandstone. Lacustrine.|
13586|Murteree Shale|67402|5|Briefly described|p90, p90 fig CPR4||BD|Cooper Basin. 50-100m thick. Distal lacustrine deposits. Forms regionally extensive seal to the Patchawarra Formation. See also p91 tbl CPR1, p92, p93, p96, p98, p101 tbl CPR2.||Gidgealpa Group||Overlies the Patchawarra Formation. Overlain by the Epsilon Formation.|Predominantly laminated, argillaceous siltstone and minor thinly bedded, fine-grained sandstones.|
13586|Murteree Shale|68068|5|Briefly described|Map legend|Early Permian|Early Permian|Cooper Basin (subsurface only). Lacustrine, cyclic oxic to anoxic conditions.||Unit in Gidgealpa Group.||Conformably overlies Patchawarra Formation. Is overlain conformably by Epsilon Formation.|Dark grey, interbedded, carbonaceous mudstone and siltstone with minor sandstone, characteristically fine-grained variably pyritic and muscovite; laminated and calcareous.|
13586|Murteree Shale|68731|5|Briefly described|p200 Fig 3.110, p204, p205, p206|Cisuralian|Cisuralian|Gatehouse (1972). Along with the Epsilon Formation and Roseneath Shale, the Murteree Shale replaces the Moomba Formation. < 80 m thick. Deposited in a large freshwater lake, with restricted circulation. Contains Kungurian palynofloras (Price 1997).||Of the Gidgealpa Group.||Conformably underlain by the Patchawarra Formation. Interdigitates with the Patchawarra Formation. Conformably overlain by the Epsilon Formation. Unconformably overlain by the Toolachee Formation.|Comprises dark, laminated, argillaceous siltstone and lesser fine sandstone with carbonaceous material, muscovite and fine pyrite.|
13586|Murteree Shale|69023|4|Described|p79, p81, p82 Fig.18, p84-85, p191-192|Permian|Permian|Defined by Gatehouse (1972). Widespread in Cooper Basin. 50 +/- 25m thick. Hydrocarbon source rocks. Lacustrine. Has high gamma ray and density values on wireline logs. Stratigraphic wells intersection data.||Unit in Gidgealpa Group.||Conformably overlies Patchawarra Formation. Is overlain by Epsilon Formation.|Black to dark grey-brown, laminated, argillaceous siltstone and fine-grained sandstone; disseminated carbonaceous matter, fine-grained pyrite and muscovite are characteristic.|
13586|Murteree Shale|69454|5|Briefly described|p38:4|Kungurian|Artinskian|Cooper Basin.||Gidgealpa Group.||||12-JUL-16
13586|Murteree Shale|69673|6|Mentioned|p153 fig 125|||||Gidgealpa Group||Overlain by Epsilon Formation, overlies Patchawarra Formation||
13586|Murteree Shale|69797|5|Briefly described|p17 Fig.2|Early Permian|Early Permian|Age: Artinskian - Kungurian (approximated from figure). Geol. Prov: Cooper Basin.||Gidgealpa Group||||
13586|Murteree Shale|69946|5|Briefly described|p9, p36, p45, p54|Kungurian|Artinskian|Cooper Basin. Lacustrine.||Unit in Gidgealpa Group.||Overlies Patchawarra Formation. Is overlain by Epsilon Formation.||
13586|Murteree Shale|69947|5|Briefly described|p13 Fig.7.2|Permian|Permian|Cooper Basin.||Gidgealpa Group.||||
13586|Murteree Shale|70317|6|Mentioned|p33-34, 36|Early Permian|Early Permian|Cooper Basin. Vertical section showing fracture densities.||Gidgealpa Group.||Overlies Patchawarra Formation. Is overlain by Epsilon Formation.||
13586|Murteree Shale|70823|4|Described|iv, p1, p3, p6|Kungurian|Kungurian|Cooper Basin. Hosts shale gas plays. Seismic reflection characteristics briefly discussed. Up to 90m thick. Deposited in a deep lacustrine environment. This unit contains potential source rock facies. See also p14-p15, p25-p27, p38, p40-p41, p53, p58-p59, p64, p78, p82-p83.||Gidgealpa Group||Conformably overlies and intertongues the Patchawarra Formation. Conformably overlain by the Epsilon Formation. Unconformably overlain by the Toolachee Formation.|Black to dark grey-brown argillaceous siltstone with minor fine-grained sandstone.|
13586|Murteree Shale|70824|4|Described|p1, p3, p7-p9, p28|Kungurian|Kungurian|Cooper Basin. Hosts shale gas plays. Deposited in a lacustrine environment. This unit has an average thickness of 50m but in the Nappamerri trough reaches a maximum thickness up to 90m. Forms a seal over the Patchawarra Formation. Outcrop characteristics and areal extent discussed briefly in addition to source rock geochemistry. See also p30-p32, p59-p65, p108-p109, p113, p122.||||Overlies the Patchawarra Formation. Overlain by the Epsilon Formation.|Black to dark grey-brown argillaceous siltstone with minor fine-grained sandstone.|
13586|Murteree Shale|70946|5|Briefly described|p1087, p1089-1091, p1096|Permian|Early Permian|Cooper Basin. Hosts shale gas plays. Widespread unit. Up to 92m thick, thinning northwards. HyLogging was combined with XRD and core petrology to target fracture stimulation. Deposited in lacustrine with interbedded fluvio-deltaic transgressive/regressive shoreface environments.||Gidgealpa Group.||Overlies Patchawarra Formation. Is overlain by Epsilon Formation.|Siltstones, siliceous (and sideritic in part) mudstones.|08-OCT-18
13586|Murteree Shale|71265|5|Briefly described|p589|Kungurian|Kungurian|Cooper Basin.||Gidgealpa Group.||Overlies Patchawarra Formation. Is overlain by Epsilon Formation.||
13586|Murteree Shale|71342|5|Briefly described|Ch5 p3, Ch5 p9, Ch5 p36|Artinskian|Artinskian|Cooper Basin. Deposited in a lacustrine environment.  Palynological zone is given in fig 5.3 Ch5 p36. See also Ch5 p45, Ch5 p54, Ch7 p13, Ch10 p15, Ch10 p18-p19.||Gidgealpa Group||Overlies the Patchawarra Formation. Overlain by the Epsilon Formation.||
13586|Murteree Shale|71701|5|Briefly described|p155|Kungurian|Kungurian|Cooper Basin.||Gidgealpa Group||Overlies the Patchawarra Formation. Overlain by the Epsilon Formation.||
13586|Murteree Shale|71863|6|Mentioned|p2|Paleozoic|Paleozoic|Cooper Basin.||||||
13586|Murteree Shale|72297|6|Mentioned|p742|||Cooper Basin. Acts as a regional seal.||||||
13586|Murteree Shale|73167|6|Mentioned|p662, p664|late Permian|late Permian|Cooper Basin. Deposited in an east-to-west late Permian transgression of fluvio-deltaic, shoreface and lacustrine sediments.||||||
13586|Murteree Shale|73244|6|Mentioned|p86|Permian|Permian|Cooper Basin. Fluvio-deltaic/shoreface environment.||||||
13586|Murteree Shale|73251|6|Mentioned|p62|Cisuralian|Cisuralian|Cooper Basin. Fluviodeltaic with local transgressive/regressive shoreface depositional environments. Hydrocarbon source rock.||Gidgealpa Group||Underlain by Patchawarra Formation. Overlain by and equivalent to Epsilon Formation.||
13586|Murteree Shale|73343|6|Mentioned|p337-338|Late Permian|Late Permian|Cooper Basin.||||Underlain by Patchawarra Formation. Overlain by Roseneath Shale. Equivalent to Epsilon Formation.||
13586|Murteree Shale|73479|5|Briefly described|p156 Fig.2, p159, p163, p166|Permian|Permian|Cooper Basin. Fluvio-deltaic/shoreface depositional environment. Highly efficient regional seal, eroded along western margin of the basin.|ca 264 Ma|||Overlies Patchawarra Formation||
13586|Murteree Shale|73495|6|Mentioned|p497, p499|Guadalupian|Guadalupian|Cooper Basin. Part of the REM succession.||||Underlain by Patchawarra Formation. Overlain by Epsilon Formation.||
13621|Myall Creek Formation|30804|6|Mentioned|p14|||On Table 1||||||
13621|Myall Creek Formation|31532|4|Described|Table 1|||||||||
13622|Myall Granite|41125|5|Briefly described|p32|||||||||
13685|Nairne Pyrite Member|9124|5|Briefly described|Map Legend|Cambrian|Cambrian|Of the Brown Hill Greywacke Member.||||||
13685|Nairne Pyrite Member|22840|6|Mentioned|P39|||||||||
13685|Nairne Pyrite Member|23317|5|Briefly described|380 Fig.2|||||||||
13685|Nairne Pyrite Member|23818|5|Briefly described|p101 Fig.43|Cambrian|Cambrian|Geological Province: Kanmantoo Trough. Base of the Brukunga Formation. Max. thickness: ~300 ft.||||||
13685|Nairne Pyrite Member|24465|4|Described|p355|Early Cambrian|Early Cambrian|Now incorpoarted into the Talisker Formation. Formerly called Nairne Pyrite Beds of Talisker Calc-Silicate.  Names now abandoned.||||||19-JAN-05
13685|Nairne Pyrite Member|29406|6|Mentioned|p58|||||||||
13685|Nairne Pyrite Member|30051|6|Mentioned|Fig.1|||Middle Cambrian age.||||||
13685|Nairne Pyrite Member|30052|6|Mentioned|p91|||||||||
13685|Nairne Pyrite Member|30077|6|Mentioned|p545|||||||||
13685|Nairne Pyrite Member|30255|6|Mentioned|Fig.1|||||||||
13685|Nairne Pyrite Member|30377|6|Mentioned|Table 2|||||||||
13685|Nairne Pyrite Member|30380|6|Mentioned|Table 1|||Refers to Thomson in Parkin(1969). See also P198 and Table 11||||||
13685|Nairne Pyrite Member|30381|6|Mentioned|p215|||||||||
13685|Nairne Pyrite Member|30801|6|Mentioned|p5|||Brukunga Formation. Table P5-6.||||||
13685|Nairne Pyrite Member|30807|6|Mentioned|p102|||Suggested map symbol||||||
13685|Nairne Pyrite Member|31322|6|Mentioned|p30|||Map legend||||||
13685|Nairne Pyrite Member|31923|6|Mentioned|p11|||||||||
13685|Nairne Pyrite Member|32321|6|Mentioned|Fig. 1|||||||||
13685|Nairne Pyrite Member|32432|6|Mentioned|Fig.2|||See also Table 1||||||
13685|Nairne Pyrite Member|33471|6|Mentioned|p556|||||||||
13685|Nairne Pyrite Member|33634|6|Mentioned|p561|||||||||
13685|Nairne Pyrite Member|34195|4|Described|p1|||See also PP2,3,4 etc.||||||
13685|Nairne Pyrite Member|34196|4|Described|p9|||See also PP10,16.||||||
13685|Nairne Pyrite Member|34536|6|Mentioned|Map legend|Middle Cambrian|Early Cambrian|Lower to Middle Cambrian||||||
13685|Nairne Pyrite Member|34612|6|Mentioned|Fig.43|||Kanmantoo basal marker bed.||||||
13685|Nairne Pyrite Member|34617|6|Mentioned|p2|||||||||
13685|Nairne Pyrite Member|35027|5|Briefly described|p385|||||||||
13685|Nairne Pyrite Member|36836|6|Mentioned|p39|||||||||
13685|Nairne Pyrite Member|39350|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
13685|Nairne Pyrite Member|40763|6|Mentioned|p209|||||||||
13685|Nairne Pyrite Member|40856|5|Briefly described|p312|||||||||
13685|Nairne Pyrite Member|41947|6|Mentioned|p16|||||||||
13685|Nairne Pyrite Member|42243|6|Mentioned|p211|||||||||
13685|Nairne Pyrite Member|42499|5|Briefly described|Map legend|Cambrian||||||||
13685|Nairne Pyrite Member|42505|5|Briefly described|Map legend|Cambrian||||||||
13685|Nairne Pyrite Member|44133|5|Briefly described|p15|||Of the Talisker Calc-siltstone.||||||
13685|Nairne Pyrite Member|45087|5|Briefly described|p227|||See also P230-232. Chem. analyses||||||
13685|Nairne Pyrite Member|60712|4|Described|p33-34, p30 Fig. 3, p36|Early Cambrian|Early Cambrian|Formerly Nairne Pyritic Schist, then Nairne Pyritic Formation. Mapped/remapped with various interpretations of location - Brukunga Fm initially and finally as part of Talisker Calc-silstone (Silverton Subgroup, Kanmantoo Group). Fine-grained.....||||||31-MAY-05
13685|Nairne Pyrite Member|61046|5|Briefly described|p8 Fig. 2|Early Cambrian|Early Cambrian|Of Talisker Formation (Kanmantoo Group). Pyritic metasediments, schist, calcsilicate.||||||
13685|Nairne Pyrite Member|61307|5|Briefly described|p6 Fig. 3|Cambrian|Cambrian|Of the Talisker Calc-Siltstone Formation (Kanmantoo Group). Geological Province: Adelaide Fold Belt.||||||15-JAN-08
13685|Nairne Pyrite Member|61838|5|Briefly described|p211|Cambrian|Cambrian|Of the Kanmantoo Group.||||||
13685|Nairne Pyrite Member|70865|6|Mentioned|p2|Cambrian|Cambrian|Adelaide Hills area. Previously (1950s to 1972) mined as a source of S for sulfuric acid to produce superphosphate. Pyritic beds extend over 100km. Sedimentary origin; remobilised during amphibolite-grade metamorphism.||Kanmantoo Group.|||Pyrite-rich metasediments (pelites and psammites) intruded by a 3m-thick mafic dyke. Contains a new mineral species: manganochromite, MnCr2O4 (Graham, 1978).|
13707|Namba Formation|13497|5|Briefly described|p115, p115 fig 6.33, p150-p154, |Miocene|Oligocene|Lake Eyre Basin.||||Unconformably overlies the Eyre Formation. Unconformably overlain by the Yandruwantha Sand.||
13707|Namba Formation|22459|6|Mentioned|p 17|||||||||
13707|Namba Formation|22712|5|Briefly described|p132|Tertiary|Tertiary|||||||
13707|Namba Formation|22773|6|Mentioned|p355|||||||||
13707|Namba Formation|22821|6|Mentioned|P8||Tertiary|||||||
13707|Namba Formation|22857|5|Briefly described|p355|Early Pliocene|Early Miocene|Max. thickness: ~75m. Geological Province: Lake Eyre Basin.||||||
13707|Namba Formation|22912|4|Described|32|||Geol province Lake Eyre Basin||||||
13707|Namba Formation|22931|6|Mentioned|10|||||||||
13707|Namba Formation|23154|5|Briefly described|Map Legend|Pliocene|Miocene|Geological Province - Lake Eyre Basin - Callabonna Basin.||||||
13707|Namba Formation|23155|4|Described|p34|||Little palaeontological information avaliable hence unit is identified by lithological correlation and continuity with similar sediments to the south. On FROME, ages established from palynofloras - latest Oligocene-?Late Miocene to Pliocene.||||||
13707|Namba Formation|23189|6|Mentioned|Table1p290,290,295||Middle Miocene|||||||
13707|Namba Formation|23339|6|Mentioned|5|||||||||
13707|Namba Formation|23477|5|Briefly described|p49 Fig 3|Tertiary|Tertiary|Geological Province: Curnamona Province.||||||
13707|Namba Formation|23478|5|Briefly described|p28|Pliocene|Oligocene|||||||
13707|Namba Formation|24102|5|Briefly described|p132|Late Miocene|Middle Miocene|||||||
13707|Namba Formation|24252|6|Mentioned|p299|Miocene|Miocene|||||||
13707|Namba Formation|24566|5|Briefly described|p113|Late Miocene|Middle Miocene|Low energy lacustrine facies. Geological Province: Frome Embayment.||||||03-MAY-05
13707|Namba Formation|29660|6|Mentioned|p6|||||||||
13707|Namba Formation|30055|6|Mentioned|p151|||Minerology P159.||||||
13707|Namba Formation|30056|2|Defined|p129|middle Miocene|middle Miocene|||||||
13707|Namba Formation|30920|6|Mentioned|Map legend|Miocene|Miocene|||||||
13707|Namba Formation|32121|6|Mentioned|p422|||||||||
13707|Namba Formation|32816|6|Mentioned|p85|||||||||
13707|Namba Formation|34882|6|Mentioned|p81|||||||||
13707|Namba Formation|35080|6|Mentioned|p14|||||||||
13707|Namba Formation|35619|6|Mentioned|p309|||||||||
13707|Namba Formation|35857|6|Mentioned|p197|||||||||
13707|Namba Formation|36213|6|Mentioned|p85|||||||||
13707|Namba Formation|36618|6|Mentioned|p9|||||||||
13707|Namba Formation|36620|5|Briefly described|Fig.1|||See also P24.||||||
13707|Namba Formation|36966|6|Mentioned|p86|||||||||
13707|Namba Formation|37062|6|Mentioned|p199|||||||||
13707|Namba Formation|37678|6|Mentioned|p243|||||||||
13707|Namba Formation|38682|6|Mentioned|Fig.3|||||||||
13707|Namba Formation|38982|5|Briefly described|p64|||||||||
13707|Namba Formation|39085|6|Mentioned|p13|||||||||
13707|Namba Formation|39322|6|Mentioned|Fig.2|||||||||
13707|Namba Formation|39666|6|Mentioned|p114|||||||||
13707|Namba Formation|39804|5|Briefly described|p163|||||||||
13707|Namba Formation|40664|6|Mentioned|p246|||||||||
13707|Namba Formation|40754|6|Mentioned|p10|||||||||
13707|Namba Formation|40755|5|Briefly described|p43|||||||||
13707|Namba Formation|40756|5|Briefly described|p3|||||||||
13707|Namba Formation|40757|3|Fully described|p75|||||||||
13707|Namba Formation|40758|6|Mentioned|p88|||||||||
13707|Namba Formation|40914|6|Mentioned|Map legend|Cenozoic|Cenozoic|||||||19-NOV-08
13707|Namba Formation|40926|6|Mentioned|Table 3|||||||||
13707|Namba Formation|41125|6|Mentioned|p34|||||||||
13707|Namba Formation|41537|6|Mentioned|p348|||See also Fig.2||||||
13707|Namba Formation|42090|5|Briefly described|p25|||||||||
13707|Namba Formation|42205|5|Briefly described|p246|||See also Fig.1||||||
13707|Namba Formation|42375|5|Briefly described|p26|Neogene||Callabonna Basin, Oligocene?||||||
13707|Namba Formation|42469|5|Briefly described|p39, p43|||||||||
13707|Namba Formation|42543|5|Briefly described|p4|||||||||
13707|Namba Formation|42746|5|Briefly described|p17|||Callabonna Basin||||||
13707|Namba Formation|42784|6|Mentioned|p494|||||||||
13707|Namba Formation|42813|6|Mentioned|p24|||||||||
13707|Namba Formation|42883|6|Mentioned|p8|||||||||
13707|Namba Formation|42957|6|Mentioned|p40|||||||||
13707|Namba Formation|43053|5|Briefly described|Map Legend|Pliocene|Miocene|Lacustrine dolomite, clay, sand and silt. Geological Province: Lake Eyre Basin.||||||25-MAY-05
13707|Namba Formation|43258|5|Briefly described|Map Legend|Pliocene|Miocene|||||||
13707|Namba Formation|43298|6|Mentioned|Map Legend|Pliocene|Miocene|||||||
13707|Namba Formation|44133|5|Briefly described|p193, 190 Fig. 10.30|Miocene|Miocene|Geoloigcal Province: Lake Eyre Basin. Disconformably overlies: Eyre Formation. Average Thickness: 90m.||||||
13707|Namba Formation|45128|6|Mentioned|Fig.42|||Correlation table of sediments containing Dromornithidae in Australia.||||||
13707|Namba Formation|45155|6|Mentioned|p46|||||||||
13707|Namba Formation|46815|6|Mentioned|p249|||||||||
13707|Namba Formation|46833|5|Briefly described|p53|||||||||
13707|Namba Formation|60564|4|Described|p4|Tertiary|Tertiary|Overlain by Willawortina Formation.||||||
13707|Namba Formation|60703|5|Briefly described|p704, p725 Fig.18|Early Miocene|Late Oligocene|Contains abundant gastrapod fossils. Geological Province: Lake Eyre Basin (Callabonna Sub-basin).||||||12-APR-05
13707|Namba Formation|60785|5|Briefly described|p184 Fig.1, pp197-198.   |?Serravallian|?Chattian|South Australia. Palynofloras suggest Miocene-Pliocene age (Alley et al., 1995). Woodburne et al. (1993) have suggested an age of 24-28 Ma for the Etadunna Formation (a correlate of the Namba Formation), implying a Late-Oligocene age. Has yielded fossil cetacean elements.||||Correlated with the Etadunna Formation.|Illite and kaolinite clays.|
13707|Namba Formation|60953|5|Briefly described|Map Legend|Pliocene|Miocene|Geological Province: Lake Eyre Basin.||||||
13707|Namba Formation|61108|5|Briefly described|map legend|Pliocene|Miocene|Lacustrine dolomite, clay, sand and silt. Geological Province: Lake Eyre Basin.||||||
13707|Namba Formation|61119|6|Mentioned|p124, pp128-9, p134, p137, p144, p147||Cenozoic|River, lake and estuarine sediments. Detailed descriptions of Lungfish fossil assemblages included.||||||28-MAR-12
13707|Namba Formation|61155|5|Briefly described|p4, p17|Middle Miocene|Early Miocene|Age: 23.5-12.5Ma. Max. thickness:250m. Geological Province: Tarkarooloo Basin.||||||
13707|Namba Formation|61823|5|Briefly described|p118|Pliocene|Oligocene|Lacustrine and alluvial deposits. Overlies Eyre Formation.  Geological Province: Lake Eyre Basin.||||||05-JUN-06
13707|Namba Formation|62592|5|Briefly described|p18.|Tertiary|Tertiary|Thin sedimentary cover, hosting roll-front uranium deposits including Honeymoon, Goulds Dam and Beverley.||||||
13707|Namba Formation|62724|5|Briefly described|p16 Fig. 2|Tertiary|Tertiary|Clay, sand, dolomite. Geological Province: Curnamona Province.||||||07-FEB-11
13707|Namba Formation|63102|4|Described|p8,62,71,74|Miocene|Miocene|Geological province: Curnamona Province. Of Callabonna Sub-basin. Widespread and directly overlies highly weathered basement in the southern Benagerie Ridge. Deposited in a low energy environment over the Eyre Formation.||||Underlain by Eyre Formation.|Fine clastics, olive to grey coloured clay, sandy clay and silts.|
13707|Namba Formation|65194|5|Briefly described|p36-37, p44-45, p47, p171|Miocene|Miocene|Lake Eyre Basin. Overlies Eyre Formation; is overlain by Willawortina Formation. Shown as including Alpha Mudstone, Beverley sands and Beverley clay. Thick clays act as an aquaclude, sealing the underlying Eyre Formation sands. Fills palaeovalleys which host uranium orebodies.||||||
13707|Namba Formation|65484|6|Mentioned|p 28,30, p29 Fig 2|Tertiary|Tertiary|Coarse sandy and gravel facies, fluvial and lacustrine.||||||
13707|Namba Formation|65925|4|Described|p44, pp49-65, p79, Appendix 2.|Miocene|Oligocene|Callabonna Sub-basin. Hosts the Beverley uranium deposit. Average thickness 90m. Equivalent to Etadunna Formation. Deposited in a fluvial lacustrine environment with meandering streams and billabongs.|c.24 Ma to 4-6 Ma.||Comprises Alpha Mudstone, Beverley Sands, Beverley Clay.|Disconformably overlies Eyre Formation and unconformably overlies Bulldog Shale. Is overlain by Willawortina Formation.|Sand, fine to medium-grained, poorly sorted, angular; silt, thin dolomite, oolitic dolomite interbeds. Shallow, brackish to fresh water lakes.|
13707|Namba Formation|66131|4|Described|p240, p242 Fig.2, p244 Fig.4, p245|Miocene|Oligocene|See also p255, p259. Callabonna Sub-basin. Defined by Callen and Tedford (1976). ~90-170 m thick. Contains abundant fossils: invertebrates in carbonate, vertebrates in upper clayey parts. Latest Oligocene to Miocene in age.||||Disconformably overlies Eyre Formation.|Comprises alternating fine to medium, poorly sorted sand, silt and clay, thin dolomite and limy, often oolitic dolomite. Silcrete capping.|
13707|Namba Formation|66303|5|Briefly described|pp27-28, p31 Fig.5, p33.|Paleogene|Paleogene|Lake Eyre Basin. Middle to Late Miocene. Palynological samples were few due to poor preservation and/or absence.||||Disconformably overlies Eyre Formation. Is overlain by Willawortina Formation.|Dominantly olive-grey clay, silt and mudstone.|
13707|Namba Formation|66518|5|Briefly described|p19 Fig.4, p20.|Miocene|Miocene|Lake Eyre Basin. Movement along faults (including the Poontana Fault) allowed thickening of these widespread fluviolacustrine deposits. The Beverley uranium deposit developed in a meandering channel within this Formation.||||Unconformably overlies Eyre Formation. Is overlain by Millyera Formation and possibly unconformably by the Willawortina Formation.|Clay, silt, sand and carbonate units.|
13707|Namba Formation|66573|6|Mentioned|p873|||Correlative of the Etadunna Formation.||||||
13707|Namba Formation|66623|6|Mentioned|p282.|||Lateral equivalent of Etadunna Formation; tentatively correlated with Doonbara Formation in NSW (Wopfner, 1974).||||||21-MAY-13
13707|Namba Formation|67462|5|Briefly described|Map legend.|Miocene|Miocene|Callabonna Sub-basin, Lake Eyre Basin.||||||
13707|Namba Formation|68068|5|Briefly described|Map legend|Pliocene|Late Oligocene|Callabonna Sub-basin, Lake Eyre Basin. Equivalent to Etadunna Formation to the west and northwest. Commonly silcreted.|||||White, very fine-grained dolomite interbedded with olive-grey clay (palygorskite) near base; swelling clay with gypsum nodules; interbedded indurated dark sandy claystone; greenish laminated silt and fine sand; bioturbated.|
13707|Namba Formation|68157|6|Mentioned|p1, p17-25|Miocene|Miocene|Hosts the Beverley sandstone-hosted uranium deposit. Includes detrital zircons aged 1576 +/- 5 Ma, ~425 Ma and ~285 Ma, as well as other smaller groupings. Also includes informal Beverley sands and Alpha mudstone.|||Includes Beverley Clay.||Includes coarse-grained sandstone, clay and mudstone.|
13707|Namba Formation|68715|6|Mentioned|p29, p29 Fig.6, p32 Fig.6|Neogene|Neogene|||||Unconformably overlies Eyre Formation.|Includes fluvial gravels.|07-APR-17
13707|Namba Formation|68821|4|Described|p296, p307|Serravallian|Chattian|Consists largely of immature fluvio-lacustrine sand, silt, and clay deposited in an alkaline and anoxic environment. Includes levels of pyritic laminated carbonaceous mud and fossils - gastropods, ostracods, algae, fish, reptiles, birds and mammals.|26 - 12 Ma|||Locally underlain by the Eyre Formation.|Consists of quartz (< 50%), kaolinte (< 40%), feldspar (< 15%), mica (< 15%), smectite(< 5%), illite (a few %), palygorskite and dolomite, gypsum and alunite.|
13707|Namba Formation|69001|5|Briefly described|p22, p23, p45, p66, p70|Pliocene|Oligocene|Late Oligocene to Early Pliocene.|||||Comprises lacustrine and fluvial sand, silt and clay.|
13707|Namba Formation|69019|5|Briefly described|p83 Fig.20, p94 Fig.24, p110-113.|Pliocene|Oligocene|Of Callen and Tedford (1976). Type section is in Yalkalpo 1 drillhole. Callabonna Sub-basin. Thickness to 109.5 m. Extensive fossil fauna listed.||||Unconformably overlies Eyre Formation. Contemporaneous with Etadunna Formation.|Interbedded indurated dark sandy claystone with sand, with thin interbeds of dolomite and palygorskite clay; overlain by swelling clay with ochre mottling and interbedded laminated silt with fine angular sand; silcrete-porcellanite upper surface.|
13707|Namba Formation|69023|4|Described|p79, p87, p101, p109, p112, p117-120|Miocene|Oligocene|See also p125-126, p133, p136, p140, p142, p153, p161, p193. Of Callen and Tedford (1976). Lake Eyre Basin. Average thickness c.90m; maximum >158m. Surface commonly silicified. Diverse and diagnostic vertebrate fossils listed. Similar vertebrate and pollen fossils to Etadunna Formation. Weathering has formed porcellanite. Local Holocene gypcrete and gypsum caps. Contains beds of palygorskite clay, usually associated with basal dolomite. Probable source (with Eyre Formation) of Yandruwantha Sand. Stratigraphic wells intersection data.||||Unconformably overlies Eyre Formation. Is overlain by Willawortina Formation, by Millyera Formation disconformably and by Yandruwantha Sand unconformably. Time-equivalent of Etadunna Formation.|Dark grey to olive clay, with ochre mottling and interbedded white to yellow silt to coarse sand; fine clayey and arenaceous clastics dominate; local white very fine-grained dolomite; local green-grey to black carboniferous to manganiferous clays.|
13707|Namba Formation|69458|5|Briefly described|p42:16, 22|Miocene|Oligocene|Lake Eyre Basin. Extensive shallow, alkaline lacustrine to fluvial deposits. Lower parts contain a vertebrate assemblage with affinities with the Pwerte Marnte Marnte fauna.||||Correlated with Ulta Limestone.|Interbedded sandstone, siltstone, shale and locally developed dolostone.|12-JUL-16
13707|Namba Formation|69562|5|Briefly described|p662 Tb.2, p663 Fig.2, p664 Tb.4|Miocene|Oligocene|See also p666 Fig.3, p667 Fig.4, p668-669, p674-676, p679-684. Lake Eyre Basin. Deposition in paleovalleys. Hosts the Beverley uranium deposit. Overall low permeability. Electrical conductivity value used in forward modelling: 300 mS/m.|c.28 Ma.||Includes Alpha Mudstone, Beverley Sands and Beverley Clay.|Overlies Eyre Formation. Is overlain unconformably by Willawortina Formation.|Clayey overbank sediments; also contains alkaline clays and sandy lenses.|06-APR-22
13707|Namba Formation|69568|5|Briefly described|p443-444|Miocene|Miocene|Lake Frome region, Lake Eyre Basin. Lacustrine, alluvial and other low-relief environments.||||Disconformably overlies Eyre Formation. Is overlain by Willawortina Formation.|Angular immature sands and silts with minor conglomerates, black carbonaceous clays and green-grey clays with some dolomites and lignite. Capped by silcrete in Lake Frome area.|
13707|Namba Formation|69572|6|Mentioned|p1190|Oligocene|Oligocene|Contains fossil koalas of the Madakoala Genus.||||||
13707|Namba Formation|69654|6|Mentioned|p4|||Curnamona Province.||||||
13707|Namba Formation|69946|5|Briefly described|p29, p129|Miocene|Oligocene|Callabonna Sub-basin, Lake Eyre Basin. Krieg et al. (1990). Up to 210m thick.|||||Carbonate and clastics from evaporation of magnesian lakes.|
13707|Namba Formation|69947|5|Briefly described|p13 Fig.7.2|Miocene|Oligocene|Callabonna Sub-basin, Lake Eyre Basin.||||||
13707|Namba Formation|70340|5|Briefly described|map legend|Pliocene|Oligocene||||||Sand, fine to medium-grained, poorly sorted, angular, silt, thin dolomite, oolitic dolomite interbeds. Shallow, brackish to fresh water lakes.|
13707|Namba Formation|70383|5|Briefly described|p45, p52|Miocene|Oligocene|Lake Eyre Basin. Mixed lacustrine, fluvial and basin margin colluvium. Detrital zircon maximum depositional age. A similar determination is an ICPMS age of c.256 +/- 10 Ma by Wulser (2009).|<256 +/- 3 Ma (SHRIMP; Cross et al., 2010).|||Overlies Eyre Formation.||
13707|Namba Formation|70384|5|Briefly described|Map legend.|Pliocene|Oligocene|Callabonna Sub-basin, Lake Eyre Basin. The lower unit only occurs subsurface: interbedded indurated dark sandy claystone with skew planes, and sand (fine to coarse, low sphericity, subrounded, polished); structures like upper unit, burrows less evident; rare vertebrate, invertebrate and plant fossils; white very fine-grained dolomite interbedded with olive-grey clay (palygorskite) near base.|||||Upper unit: olive-grey (weathers black) swelling clay, gypsum nodules near top; greenish laminated silt and fine angular well-sorted sand; white lacustrine oolitic and conglomeratic dolomite nodules and beds; bioturbated; rare invertebrate fossils.|
13707|Namba Formation|70657|5|Briefly described|p9 Fig.3, p68, p77-78, p80|Miocene|Miocene|Widespread unit. Directly overlies highly weathered basement. Relatively high Zn content makes surface geochemical prospecting difficult.||||Overlies Eyre Formation.|Olive to grey clay (mainly smectites), sandy clay, silt, dolomite.|
13707|Namba Formation|70658|6|Mentioned|p14|Tertiary|Tertiary||||||Clay, sand, dolomite.|
13707|Namba Formation|70821|5|Briefly described|p25, p82|Miocene|Oligocene|Callen et al. (1975). Lake Eyre Basin (NSW, QLD).||||Equivalent to Whitula Formation.||
13707|Namba Formation|70823|5|Briefly described|p47|Late Oligocene|Late Oligocene|Callabonna Sub-basin. Maximum thickness of 210m.|ca 28 Ma||||Clay, fine-grained sand, carbonate and minor conglomerate.|
13707|Namba Formation|71317|5|Briefly described|p144|||||||Equivalent to the Garford Formation.||
13707|Namba Formation|71342|5|Briefly described|Ch5 p29, Ch5 p130, Ch7 p13|Miocene|Oligocene|Lake Eyre Basin. Maximum thickness of 210m in the Cooper region.||||Unconformably overlies the Eyre Formation. Unconformably overlain by the Yandruwantha Sand.|Carbonates and clastic rocks.|
13707|Namba Formation|72456|5|Briefly described|Map Legend|Pliocene|Oligocene|Marree 1:250k map sheet.  Deposited in shallow, brackish to fresh water lakes.|||||Sand, fine to medium-grained, poorly sorted, angular, silt, thin dolomite, oolitic dolomite interbeds.|
13707|Namba Formation|72457|5|Briefly described|p91, 96, 101|Miocene|Miocene|Callabonna sub-basin.||||Overlies Eyre Formation.|Fluvial successions.|
13707|Namba Formation|72458|6|Mentioned|p4|Neogene|Neogene|Low-energy fluviatile and lacustrine sediments.||||Overlain by Willawortina Formation and Pooraka Formation.||
13707|Namba Formation|73251|4|Described|p36-46, p48-53, p55, p57-62|Miocene|Miocene|Lake Eyre Basin, Callabonna Sub-basin. [Many informal subdivisions are referred to including: 'lower member', 'upper member', 'Namba carbonate', 'Alpha mudstone', 'Alpha sequence', 'Beverley sand', 'Beverley sequence', and 'basal unit 1', as well as lower, middle, and main aquitards]. Potential detrital U reductant and potential shallow hydrocarbon source rock. Sandstone hosts Beverley U deposit. Thermally sub-mature. Includes oil-prone organic facies. Depositional environments included fluviolacustrine, shallow/brackish lacustrine, and paludal/swamp. Records suboxic/anoxic bottom-water conditions during deposition of basal strata and oxic for upper strata. Callen and Tedford (1976) nominated the Wooltana 1 drillhole as one of several type localities. Basal strata (lowermost bed of 'lower member') has a reliable palynological date of c. 23 Ma. Contains Namba [organic] facies 1 and 2. [See article for organic petrology descriptions].||||Unconformably underlain by Eyre Formation. Overlain by Willawortina Formation unconformably[?] and Millyera Formation.||
13707|Namba Formation|73281|6|Mentioned|Appendix (DIP)|||See DIP034_Welldata.xlsx.||||||
13738|Namur Sandstone|13497|3|Fully described|p26, p115, p115 fig 6.33|Jurassic|Jurassic|Eromanga Basin. Deposited in a low sinuosity fluvial environment. See also p138 fig 8.17, p139 fig 8.18, p141, p146, p151 fig 9.23, p152 fig 9.25,  p171, p173, p184, p216. Incorrectly referred to as the obsolete Namur Sandstone Member in the App, p216.||||Overlies the Adori Sandstone and the Westbourne Formation. Overlain by the McKinlay Member, Murta Formation and the Cadna-owie Formation.|Sandstone.|
13738|Namur Sandstone|13516|6|Mentioned|p167 fig 10, p171 fig 12|Early Cretaceous|Late Jurassic|In Eromanga Basin.||||||
13738|Namur Sandstone|22839|6|Mentioned|P33|||||||||
13738|Namur Sandstone|22883|5|Briefly described|P31, Fig2||Late Jurassic|Overlying unit is Murta Formation, underlying unit is Birkhead Formation.||||||16-SEP-08
13738|Namur Sandstone|22909|5|Briefly described|42|||||||||
13738|Namur Sandstone|23054|6|Mentioned|Fig5p22|||||||||
13738|Namur Sandstone|23155|2|Defined|p26-27 & Fig 15 p28|Early Cretaceous|Late Jurassic|For Max. Thickness of type section see Fig 15 on p28.  For location of type section and details of previous names see p27.||||||16-APR-08
13738|Namur Sandstone|23375|4|Described|Fig2 p265,268-271|Berriasian|Oxfordian|Laterally equivalent to lower-middle Hooray Sandstone, Westbourne Formation and Adori Sandstone. IN the Eromanga Basin.||||||17-JAN-08
13738|Namur Sandstone|23849|5|Briefly described|p781|Early Cretaceous|Early Cretaceous|Geological Province: Eromanga Basin.||||||
13738|Namur Sandstone|23982|5|Briefly described|p58 Fig.18|||Geological Province: Eromanga Basin.||||||
13738|Namur Sandstone|24092|5|Briefly described|p8 Fig.3|||Geological Province: Eromanga Basin.||||||
13738|Namur Sandstone|24204|5|Briefly described|p266|Jurassic|Jurassic|Geological Province: Eromanga Basin.||||||
13738|Namur Sandstone|24210|5|Briefly described|p133 Fig. 2|Early Cretaceous|Late Jurassic|Geological Province: Eromanga Basin.||||||
13738|Namur Sandstone|24372|6|Mentioned|p22|||Geological Province: Cooper Basin.||||||
13738|Namur Sandstone|24482|5|Briefly described|p44|Cretaceous|Jurassic|Geological Province: Eromanga Basin.||||||
13738|Namur Sandstone|37287|6|Mentioned|p33|||||||||
13738|Namur Sandstone|38108|6|Mentioned|Table 1|||||||||
13738|Namur Sandstone|38730|6|Mentioned|p29|||||||||
13738|Namur Sandstone|40030|6|Mentioned|p131|||||||||
13738|Namur Sandstone|40670|6|Mentioned|p213|||||||||
13738|Namur Sandstone|41061|6|Mentioned|Fig.6|||||||||
13738|Namur Sandstone|41099|6|Mentioned|Fig.6|||||||||
13738|Namur Sandstone|41123|6|Mentioned|p180|||||||||
13738|Namur Sandstone|41216|6|Mentioned|p300|||||||||
13738|Namur Sandstone|41705|6|Mentioned|p122|||||||||
13738|Namur Sandstone|41712|6|Mentioned|p282|||||||||
13738|Namur Sandstone|41724|6|Mentioned|p382|||||||||
13738|Namur Sandstone|42357|6|Mentioned|p11|||||||||
13738|Namur Sandstone|43711|6|Mentioned|p18|||||||||
13738|Namur Sandstone|60717|5|Briefly described|p40 Fig. 2|Late Jurassic|Late Jurassic|Overlies Birkhead Formation; overlain by Murta Formation; lateral to Adori Sandstone, and possibly to Algebuckina Sandstone also. Geological Province: Eromanga  Basin.||||||31-JAN-08
13738|Namur Sandstone|61613|6|Mentioned|p282, p284|Jurassic|Jurassic|||||||07-FEB-11
13738|Namur Sandstone|61614|6|Mentioned|p295, p290 Fig. 2|Early Cretaceous|Late Jurassic|Geological Province: Eromanga Basin.||||||17-MAR-09
13738|Namur Sandstone|61615|6|Mentioned|p302 Fig. 2|Early Cretaceous|Late Jurassic|Geological Province: Eromanga Basin.||||||07-FEB-11
13738|Namur Sandstone|62028|6|Mentioned|p10|||Abbreviation? of Namur Sandstone Member.||||||26-FEB-08
13738|Namur Sandstone|62029|5|Briefly described|p15 Fig. 4|Cretaceous|Cretaceous|||||||
13738|Namur Sandstone|62537|6|Mentioned|p191 Fig.2. |Early Cretaceous|Early Cretaceous|Eromanga Basin.||||Overlies Algebuckina Sandstone. Is overlain by Bulldog Shale and Cadna-owie Formation.||
13738|Namur Sandstone|63979|5|Briefly described|Fig. 44|Berriasian|Oxford|Supersedes "Namur Sandstone member". As a formally defined SA unit, this encompasses the Queensland interval Adori Sandstone-Westbourne Formation-Hooray Sandstone.||||||07-FEB-11
13738|Namur Sandstone|64048|6|Mentioned|p71|||Superseded "Namur Sandstone Member" of the Mooga Formation in South Australia. Mooga Formation now obsolete. Geological Province: Eromanga Basin.||||||07-FEB-11
13738|Namur Sandstone|64197|6|Mentioned|p630 Fig.6|Late Jurassic|Late Jurassic|Eromanga Basin.||||Is overlain by Murta Member.||
13738|Namur Sandstone|64665|5|Briefly described|p53 Fig.2, p62.|Early Cretaceous|Late Jurassic|Eromanga Basin.||||Is overlain by Murta Formation.||
13738|Namur Sandstone|65238|5|Briefly described|p10|||Geological province: Eromanga Basin. Sheet sandstone of fluvial origin.||||||
13738|Namur Sandstone|65385|5|Briefly described|pS134 Fig.7|Early Cretaceous|Late Jurassic|Of Eromanga Basin. Overlain by Murta Formation. Unit shown to include unconformity around Jurassic-Cretaceous boundary? Quartz-rich sediment. See also "upper Namur Sandstone".||||||08-MAR-12
13738|Namur Sandstone|65489|5|Briefly described|p11, p15, p17, p47, p49, p61, p73, p96|Early Cretaceous|Jurassic|See also p154-155, p158-160. Eromanga Basin. Fair to excellent reservoir quality. Predominantly anticlinal traps. Gas and oil reservoir accounting for 30% and 15% respectively of the Basin's production.||||Overlies Westbourne Formation. Is overlain by Murta Formation.|Braided fluvial sandstone.|
13738|Namur Sandstone|65925|5|Briefly described|Appendix 2.||||||||White to pale grey, fine- to medium-grained, crossbedded and quartzose sandstone; minor siltstone and mudstone.|
13738|Namur Sandstone|66529|6|Mentioned|p12 Fig.5|||Eromanga Basin.||||Overlies Injune Creek Group. Is overlain by Murta Formation.||
13738|Namur Sandstone|66623|3|Fully described|p34, p102, pp238-249. |Cretaceous|Cretaceous|Name introduced by Mount (1981) as member of Mooga Formation; formation status by Gravestock et al. (1995). Partly equivalent to Gum Vale Beds (Rose and Brunker 1969) and Warratta Sandstone Member (Moreton 1982). Equivalent to lower part of Hooray Sandstone and Algebuckina Sandstone in Queensland. Overall, an upward-fining sequence. Variably ferruginised and cross-bedded. Thickness varies to 1200 m. Basal section hosts flaky alluvial gold and nuggets. Silicified wood locally abundant.||||Unconformably overlies Nundora and Depot Glen Formations, as well as Tibooburra Granodiorite. Is overlain by Cadna-owie Formation and, locally, by Eyre Formation and Cordillo Silcrete.|Basal quartz pebble conglomerate; non-marine, medium- to coarse-grained, pale grey and buff, cross-bedded quartzose and pebbly sandstone; minor thin claystone lenses.|
13738|Namur Sandstone|66915|5|Briefly described|p6 Fig.3|Early Cretaceous|Late Jurassic|Eromanga Basin. In Fig.3 also shows "upper Namur Sandstone".||||||
13738|Namur Sandstone|66917|5|Briefly described|Map legend|Cretaceous|Cretaceous|||Unit in Rolling Downs Group.|||Non-marine, medium- to coarse-grained, pale grey and buff, cross-bedded quartzose and pebbly sandstone with conglomerate beds and minor thin claystone lenses.|
13738|Namur Sandstone|66918|5|Briefly described|Map legend|Cretaceous|Cretaceous|The ferruginous sandstone and conglomerate is mapped separately.|||||Non-marine, medium- to coarse-grained, pale grey and buff, cross-bedded quartzose and pebbly sandstone with conglomerate beds and minor thin claystone lenses; ferruginous sandstone, conglomerate.|
13738|Namur Sandstone|66920|5|Briefly described|Map legend|Cretaceous|Cretaceous|The ferruginous and  weathered units are mapped separately.|||||Non-marine, medium- to coarse-grained, pale grey and buff, cross-bedded quartzose and pebbly sandstone with conglomerate beds and minor thin claystone lenses; ferruginous sandstone, conglomerate; deeply weathered, kaolinised sandstone and claystone.|
13738|Namur Sandstone|66921|5|Briefly described|Map legend|Cretaceous|Cretaceous||||||Non-marine, medium- to coarse-grained, pale grey and buff, cross-bedded quartzose and pebbly sandstone with conglomerate beds and minor thin claystone lenses.|
13738|Namur Sandstone|66922|5|Briefly described|Map legend|Cretaceous|Cretaceous||||||Non-marine, medium- to coarse-grained, pale grey and buff, cross-bedded quartzose and pebbly sandstone with conglomerate beds and minor thin claystone lenses.|
13738|Namur Sandstone|67207|5|Briefly described|Map legend.|Cretaceous|Cretaceous||||||Non-marine, medium- to coarse-grained, pale grey and buff, cross-bedded quartzose and pebbly sandstone with conglomerate beds and minor thin claystone lenses.|
13738|Namur Sandstone|67208|5|Briefly described|Map legend.|Cretaceous|Cretaceous||||||Non-marine, medium- to coarse-grained, pale grey and buff, cross-bedded quartzose and pebbly sandstone with conglomerate beds and minor thin claystone lenses.|
13738|Namur Sandstone|67209|5|Briefly described|Map legend.|Cretaceous|Cretaceous|||||Overlies Easter Monday Formation of the Warratta Group. Is overlain by Wyandra Sandstone Member of Cadna-owie Formation.|Non-marine, medium- to coarse-grained, pale grey and buff, cross-bedded quartzose and pebbly sandstone with conglomerate beds and minor thin claystone lenses.|
13738|Namur Sandstone|67210|5|Briefly described|Map legend.|Cretaceous|Cretaceous||||||Non-marine, medium- to coarse-grained, pale grey and buff, cross-bedded quartzose and pebbly sandstone with conglomerate beds and minor thin claystone lenses.|
13738|Namur Sandstone|67211|5|Briefly described|Map legend.|Cretaceous|Cretaceous||||||Non-marine, medium- to coarse-grained, pale grey and buff, cross-bedded quartzose and pebbly sandstone with conglomerate beds and minor thin claystone lenses.|
13738|Namur Sandstone|67402|6|Mentioned|p109 tbl ERO1|||||||Equivalent to the Hooray Sandstone and Murta Formation.||
13738|Namur Sandstone|68068|5|Briefly described|Map legend|Early Cretaceous|Late Jurassic|Eromanga Basin. Subsurface only. Is replaced by Algebuckina Sandstone as it pinches out at Eromanga Basin margin. Sandy lacustrine and braided river deposits.||||Overlies Birkhead Formation. Is overlain by Murta Formation.|White, fine- to coarse-grained sandstone, flat to cross-bedded, locally with calcareous cement, channel lag conglomerate; siltstone interbeds, especially in middle part; minor mudstone and coal stringers.|
13738|Namur Sandstone|68135|5|Briefly described|p52 Fig.2b|Early Cretaceous|Tithonian|Eromanga Basin.||||Unconformably overlies Westbourne Formation.|Predominantly sandstone.|
13738|Namur Sandstone|68731|6|Mentioned|pp209-211|||||||||
13738|Namur Sandstone|69001|6|Mentioned|p16|||See also Namur sandstone. Interpretations by the NSW DPI of the Namur Sandstone flanking many of the inliers are broadly grouped in this study within the Algebuckina Sandstone and equivalent units.||||||
13738|Namur Sandstone|69019|5|Briefly described|p85 Fig.21.|Early Cretaceous|Early Cretaceous|Southern Eromanga Basin.||||Overlies Westbourne Formation. Is overlain by Murta Formation.||
13738|Namur Sandstone|69023|4|Described|p79, p89 Fig.20, p91, p191-192|Hauterivian|Berriasian|Named after Delhi Petroleum exploration well Namur 1 (Mount, 1981) as Namur Sandstone Member of Mooga Formation (Nugent, 1969). This last name has been abandoned (Gravestock et al.,1995) as the Namur Sandstone Member was elevated to Formation status (Callen et al.,1994; Gravestock et al.,1995; after Martin (1983). Eromanga Basin. Thickness from ~120 to ~194m, thinning to W. Stratigraphic wells intersection data.||||Overlies Birkhead Formation. Intertongues with Westbourne Formation. Passes laterally into Algebuckina Sandstone. Is overlain by Murta Formation.|White to pale grey, flat and cross-bedded, fine- to coarse-grained, quartzose sandstone; minor siltstone and mudstone interbeds; channel lag conglomerates. Locally strongly cemented with calcite.|
13738|Namur Sandstone|69454|6|Mentioned|p38:13|||Cooper Basin. With the overlying Murta Formation, is equivalent to the upper Algebuckina Sandstone in the Poolowanna Trough.||||||12-JUL-16
13738|Namur Sandstone|69457|6|Mentioned|p41:3-4, 7|||Eromanga Basin.||||Is overlain by Murta Formation.||12-JUL-16
13738|Namur Sandstone|69594|5|Briefly described|p519, p525-527, p532, p573|Tithonian|Tithonian|Eromanga Basin. Along the SA border, the Namur Sandstone, Westbourne Formation and Adori Sandstone cannot be delineated and the succession is called the Namur Sandstone. In QLD, where differentiation is possible, the Westbourne Formation is overlain by the Hooray Sandstone, equivalent to the topmost, Murta Formation overlying the rest of the upper part of the Namur Sandstone. This unit separating Westbourne and Murta Formations is referred to in QLD as the [informally named] upper Namur Sandstone, echoing the obsolete Namur Sandstone Member (Gray et al. 2002). A significant hydrocarbon reservoir.||||?Overlies Birkhead and Westbourne Formations unconformably. Passes laterally into Westbourne Formation locally. Is overlain by Murta Formation.||
13738|Namur Sandstone|69673|6|Mentioned|p154, p155 fig 127|Cretaceous|Cretaceous|||||Overlies Westbourne Formation, overlain by McKinlay Member, Murta Formation||
13738|Namur Sandstone|69790|6|Mentioned|p1063 Fig.2|Cretaceous|Late Jurassic|Eromanga Basin.||||||
13738|Namur Sandstone|69797|5|Briefly described|p17 Fig.2|Early Cretaceous||Age: Late Jurassic - Early Cretaceous (approximated from figure). Geol. Prov: Eromanga Basin.||||||
13738|Namur Sandstone|69946|3|Fully described|p11, p15-17, p57-58, p61, p83-85|Early Cretaceous|Late Jurassic|Originally Mooga Formation (Nugent, 1969) or part of Hooray Sandstone; named Namur Sandstone Member by Mount (1981) after Namur 1; elevated to Formation status by Gravestock et al. (1995) with the name Mooga Formation discarded in SA. In Qld the lower part of Hooray Sandstone is an equivalent. Type section is the interval 1435.22 - 1643.48m in Strzelecki 4. Generally 40 - 240m thick. Wireline log correlations.||||Conformably overlies Birkhead and Westbourne Formations. Intertongues with overlying Murta Formation or McKinlay Member. Lateral equivalent of Algebuckina Sandstone.|White to pale grey, fine- to coarse-grained sandstone with minor interbedded siltstone and mudstone; conglomeratic interbeds consist of lithic and quartz pebbles, carbonaceous mudstone intraclasts; locally strongly cemented by diagenetic calcite.|
13738|Namur Sandstone|69947|5|Briefly described|p3, p7-8, p13 Fig.7.2, p27 Fig.7.16|Early Cretaceous|Late Jurassic|See also p29 Fig.7.18. Eromanga Basin. Lowstand braided fluvial sandstones form significant hydrocarbon reservoirs. Generalised stratigraphic section.||||Conformably overlies Birkhead Formation. Intertongues with Westbourne Formation. Is overlain transitionally by McKinlay Member (Murta Formation). ?Correlates with Hooray Sandstone.|Fluvial sandstones, minor shale.|
13738|Namur Sandstone|69948|6|Mentioned|Fig.4.2|||Eromanga Basin (an intracratonic basin). Sediment thickness, sonic log, gamma ray log all shown in contrast with Otway Basin (a rift basin).||||Is overlain by Murta Formation.||
13738|Namur Sandstone|69961|5|Briefly described|Map legend|Cretaceous|Cretaceous|||Unit in Rolling Downs Group?|||Non-marine, medium- to coarse-grained, pale grey and buff, cross-bedded quartzose and pebbly sandstone with conglomerate beds and minor thin claystone lenses.|16-SEP-15
13738|Namur Sandstone|70648|5|Briefly described|Map Legend|Cretaceous|Cretaceous||||Includes 2 un-named units.||Non-marine, medium- to coarse-grained, pale grey and buff, cross-bedded quartzose and pebbly sandstone with conglomerate beds and minor thin claystone lenses. 2 un-named units: Clast supported conglomerate variant. Strongly silicified variant.|
13738|Namur Sandstone|70649|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Un-named units: Ferruginous sandstone, conglomerate. Deeply weathered, leached and kaolinised sandstone and claystone.|||Includes 2 un-named units.||Non-marine, medium- to coarse-grained, pale grey and buff, cross-bedded quartzose and pebbly sandstone with conglomerate beds and minor thin claystone lenses.|
13738|Namur Sandstone|70650|5|Briefly described|Map Legend|Cretaceous|Cretaceous||||Includes un-named unit.||Non-marine, medium- to coarse-grained, pale grey and buff, cross-bedded quartzose and pebbly sandstone with conglomerate beds and minor thin claystone lenses. Un-named unit is a strongly silicified variant.|
13738|Namur Sandstone|70652|5|Briefly described|Map Legend|Cretaceous|Cretaceous||||||Non-marine, medium- to coarse-grained, pale grey and buff, cross-bedded quartzose and pebbly sandstone with conglomerate beds and minor thin claystone lenses.|
13738|Namur Sandstone|70821|5|Briefly described|p21 Fig.2.6, p31|Early Cretaceous|Jurassic|Eromanga Basin. Previously part of the [obsolete] "Lower Hooray Sandstone". 29 m thick interval, between 439-468 m in Weilmoringle 1 well.|||Appears to include the Murta Member.|Overlies Westbourne Formation. Is overlain by Cadna-owie Formation, Murta Formation..||02-DEC-16
13738|Namur Sandstone|70823|5|Briefly described|p43-p44, p78|Early Cretaceous|Late Jurassic|Eromanga Basin.  Up to 210m thick. Deposited in a braided fluvial with intertonguing lacustrine environment.||||Intertongues with the Hutton Sandstone. Overlies the Westbourne Formation. Overlain by the Murta Formation.||
13738|Namur Sandstone|70824|5|Briefly described|p9|Cretaceous|Jurassic|Eromanga Basin.||||Overlies the Westbourne Formation. Overlain by the Cadna-owie Formation.||
13738|Namur Sandstone|71321|6|Mentioned|p15|||Of Eromanga Basin.||||||
13738|Namur Sandstone|71342|3|Fully described|Ch 1 p3, Ch 1 p6|Berriasian|Late Jurassic|Eromanga Basin. Mount (1981) named the Namur Sandstone Member after Namur 1. The unit was previously referred to as the Mooga Formation or Hooray Sandstone. Martin (1983), Gravestock et al. (1995) elevated the Namur Sandstone Member of the Mooga Formation to formation status and discarded the Mooga Formation in South Australia. Source of the majority of gas production in the Eromanga Basin. Equivalent to the lower part of the Hooray Sandstone. In Queensland this unit may be subdivided into the Adori Sandstone, Westbourne Formation and Namur Sandstone. A type section in Strzelecki 4 is given (Gravestock et al., 1995). This unit is generally 40 to 240m thick in the Cooper region. Interpreted to have been deposited in a low-sinuosity fluvial environment similar to that of the Algebuckina and Hutton Sandstones. Spore-pollen zone is given in Ch5 p57. Seal and reservoir characteristics discussed in Ch11.  Laterally equivalent to the Algebuckina Sandstone. See also Ch 1 p19, Ch3 p17-p18, Ch4 p9, Ch5 p12, Ch5 p14-p17, Ch5 p32, Ch5 p57-p58, Ch5 p82-p84, Ch6 p5-p7, Ch7 p7-p8, Ch7 p10, Ch7 p13, Ch7 p29, Ch8 p3, Ch8 p10, Ch8 p17, Ch9 p5, Ch9 p10-p11, Ch10 tbl 10.1, Ch10 p6-p8, Ch10 p14, Ch10 p18-p20, Ch11 p3-p5, Ch11 p7-p8, Ch11 p16, Ch12 p2, Ch12 p5-p6, Ch12 p15, Ch13 p2-p7, Ch13 p9-p10, Ch13 p18, Ch13 p21-p22, Ch13 p26-p27, Ch13 p29, Ch13 p31, Ch14 p3, Ch14 p5-p7.||||Conformably overlies the Birkhead Formation. Overlain by the Cadna-owie Formation. Intertongues with or is overlain by the Westbourne Formation (lower) and the Murta Formation or McKinlay Member.|White to pale grey, fine to coarse-grained sandstone with minor interbedded siltstone and mudstone. Conglomeratic interbeds consist of lithic and quartz pebbles, carbonaceous mudstone intraclasts and carbonised plant fragments.|
13738|Namur Sandstone|71415|5|Briefly described|p11-14|Cretaceous|Cretaceous|Geological province: SW Thomson Orogen. Of the Kooneberry Belt; of Eromanga Basin. Probably Cretaceous in age (Exon and Senior 1976; Hill et al. 2008). LA-ICPMS zircon age populations show peaks at c. 575, c. 510, 480+\-12 and 430+\-6 Ma. Also includes small Proterozoic zircon populations at c. 2020-900 Ma, and minor Archean c. 3330 to 2555 Ma populations.||||Overlain by Cadna-owie Formation. Laterally equivalent to Algebuckina Sandstone.||19-AUG-19
13738|Namur Sandstone|71863|6|Mentioned|p5|Valanginian|Tithonian|Eromanga Basin.||||Overlain by the Murta Formation.||
13738|Namur Sandstone|72298|5|Briefly described|p801|Cretaceous|Jurassic|Eromanga Basin (SA,QLD). Main confined aquifers, generally producing flowing artesian water bores.||||Overlies Westbourne FZ (Injune Creek Group). Is overlain by Murta FZ.||
13738|Namur Sandstone|72921|5|Briefly described|p15 Fig.2.|Cretaceous|Late Jurassic|Shown with Hooray Sandstone as located in the Eromanga Basin.||||Unconformably overlies Westbourne Formation.||
13738|Namur Sandstone|73167|6|Mentioned|p664 Fig. 2|Cretaceous|Jurassic|Eromanga Basin. Contains oil.||||||
13738|Namur Sandstone|73251|6|Mentioned|p49, p55-56, p62|Cretaceous|Late Jurassic|Eromanga Basin. Contains hydrocarbon accumulations to which the Murta Formation contributed.||||Underlain by Birkhead and Westbourne formations. Equivalent to Westbourne Formation, Adori Sandstone and Algebuckina Sandstone. Overlain by and equivalent to McKinlay Member (Murta Formation).||
13738|Namur Sandstone|73343|6|Mentioned|p337|Cretaceous|Jurassic|Eromanga Basin. Hosts oil.||||Underlain by Mooga Formation. Overlain by Cadna-owie Formation. Equivalent to Murta Member, Hooray Sandstone, and Westbourne Formation.||
13738|Namur Sandstone|73479|5|Briefly described|p156 Fig.2, p159, p164, p179|Cretaceous|Jurassic|Eromanga Basin. Braided fluvial-lacustrine depositional environment.|ca 152-140 Ma|||Overlies Mooga Formation, underlies Cadna-owie Formation||
13823|Nappamerri Group|13497|4|Described|iv, v, x, xi, xii, p63-p65, p69 fig 6.1|Late Triassic|Late Permian|Cooper Basin. Maximum thickness of 600m. Previously the Nappamerri Formation before being elevated to Group status by Channon and Wood (1989) and Powis (1989). Widespread and best developed in the Nappamerri and Patchawarra troughs where it is over 500m thick. See also p70, p104, p132 tbl 8.1, p133, p141, p144 fig 9.2, p146, p148-p153, p170, p189, p204, p216.|||Includes the Arrabury Formation, Tinchoo Formation and the Cuddapan Formation.|Conformably overlies the Toolachee Formation and the Gidgealpa Group.||
13823|Nappamerri Group|13516|6|Mentioned|p147 fig 5, p163, p171 fig 12|Triassic|Late Permian|From Cooper Basin||||||
13823|Nappamerri Group|22883|6|Mentioned|P31|Middle Triassic|Late Permian|||||||
13823|Nappamerri Group|23154|6|Mentioned|Map Legend|Triassic|Permian|Geological Province - Cooper Basin.||||||
13823|Nappamerri Group|23155|4|Described|p23|Triassic|Late Permian|Underlying unit on STRZELECKI - Gidgealpa Group (disconformity).||||||
13823|Nappamerri Group|23340|5|Briefly described|12|Triassic|Triassic|||||||
13823|Nappamerri Group|23375|6|Mentioned|p293, 294|||In the Cooper Basin..||||||20-NOV-06
13823|Nappamerri Group|23731|5|Briefly described|p71|Triassic|Triassic|Geological Province: Cooper Basin.||||||
13823|Nappamerri Group|23982|5|Briefly described|p58 Fig.18|||Geological Province: Eromanga Basin.||||||
13823|Nappamerri Group|24092|5|Briefly described|p8 Fig.3|||||||||17-JAN-08
13823|Nappamerri Group|24204|5|Briefly described|p262, 270|||Equivalent to Walkandi Group. Geological Province: Cooper Basin.||||||17-DEC-04
13823|Nappamerri Group|24210|5|Briefly described|p133 Fig. 2|Middle Triassic|Late Permian|Overlies the Toolachee Formation.  Geological Province: Cooper Basin.  See also p132.||||||
13823|Nappamerri Group|42008|1|Redefined|p269|Carnian|Tatarian|See also Fig.2, Fig.3, Fig.4||||||
13823|Nappamerri Group|42085|6|Mentioned|Fig.2 P374|||||||||
13823|Nappamerri Group|42395|5|Briefly described|Fig.13 P83|||In Qld, SA.||||||
13823|Nappamerri Group|42746|5|Briefly described|Fig.2 P4|||||||||
13823|Nappamerri Group|42999|5|Briefly described|Table 2,p90||Middle Triassic|||||||
13823|Nappamerri Group|43105|5|Briefly described|Fig.7,p13|||||||||
13823|Nappamerri Group|43570|6|Mentioned|Fig.2,p535|Scythian|Tatarian|||||||
13823|Nappamerri Group|43628|6|Mentioned|Fig.3|Late Triassic|Early Triassic|||||||
13823|Nappamerri Group|44133|4|Described|p78-79, 85|Middle Triassic|Late Permian|Geological Province: Cooper Basin. Overlies: Gidgealpa Group. Consists of: Arrabury Formation, Tinchoo Formation. Overlain by the Cuddapan Formation. Thickness:>550m.||||||17-JAN-08
13823|Nappamerri Group|60717|5|Briefly described|p40, p41|Middle Triassic|Late Permian|Includes Arrabury and Tinchoo Formations. Overlies the Gidgealpa Group. Max.  Thickness: 500m. Geological Province: Cooper Basin. See also Figure 2.||||||17-JUL-14
13823|Nappamerri Group|61015|6|Mentioned|p45|Triassic|Triassic|||||||19-APR-05
13823|Nappamerri Group|61613|6|Mentioned|p282, p282 Fig. 2|Triassic|Late Permian|Includes Arrabury and Tinchoo Formation. Geological Province: Cooper and Simpson Basins.||||||07-FEB-11
13823|Nappamerri Group|61614|6|Mentioned|p294, p295, p290 Fig. 2|Middle Triassic|Late Permian|Includes Tinchoo and Arrabury Formations. Geological Province: Cooper Basin.||||||17-MAR-09
13823|Nappamerri Group|61615|5|Briefly described|p302, p303, p302 Fig. 2, p304, p305|Late Triassic|Late Permian|Includes; Arrabury and Tinchoo Formations, Callamburra, Paning and Wimma Sandstone Members. Conformably overlies Toolachee Formation. Geological Province: Cooper Basin. Fluvial and lacustrine environments.||||||07-FEB-11
13823|Nappamerri Group|61616|6|Mentioned|p330 Fig. 2|Early Triassic|Late Permian|Includes Arrabury and Tinchoo Formations. Geological Province: Cooper Basin.||||||
13823|Nappamerri Group|62046|5|Briefly described|p125 Fig. 2|Triassic|Permian|Geological Province: Cooper-Eromanga Basins.||||||14-APR-08
13823|Nappamerri Group|62537|6|Mentioned|p191 Fig.2. |Late Triassic|Early Triassic|Cooper Basin.|||Includes Arrabury and Tinchoo Formations and Wimma Sandstone.|Overlies Gidgealpa Group.||
13823|Nappamerri Group|62730|5|Briefly described|p351, p352 Fig. 1|Late Triassic|Late Permian|Includes the Arrabury and Tinchoo Formations. Geological Province: Cooper Basin.||||||21-APR-08
13823|Nappamerri Group|63832|6|Mentioned|p131 fig 2|Changhsingian|Changhsingian|Of Cooper Basin.||||||14-MAR-14
13823|Nappamerri Group|63978|2|Defined|p7, p18, Fig. 3|Early Triassic|Late Permian|Supersedes Nappamerri Fm. Contains the Arrabury and Tinchoo Fms. Max. thick: 450m. Conformable on Toolachee Fm (Gidgealpa Gp). Unconformably overlain by Poolawanna Fm and Hutton Sandstone (Eromanga Basin), and by Cuddapan Fm. in places. In Cooper Basin.||||||07-FEB-11
13823|Nappamerri Group|63979|6|Mentioned|p31|||||||||07-FEB-11
13823|Nappamerri Group|64048|5|Briefly described|p65|Triassic|Early Triassic|Includes the Tinchoo Formation. Member units act as a seal for the Toolachee Formation reservoirs.||||||07-FEB-11
13823|Nappamerri Group|64197|6|Mentioned|p625 Fig.1c|Middle Triassic|Late Permian|Cooper Basin.|||Includes the Arrabury and Tinchoo Formations|Overlies Toolachee Formation.||
13823|Nappamerri Group|64631|6|Mentioned|p44 Fig.2.||Changhsingian|Cooper Basin. Some biostratigraphic age control.||||Overlies Toolachee Formation.||
13823|Nappamerri Group|65489|5|Briefly described|p24-25, p42, p48, p96, p130-132, p158|Middle Triassic|Permian|Cooper Basin. Reservoir for economic oil and gas. The best source rocks are thin, laterally discontinuous coals in the upper part of the unit. Also regarded as a regional seal to the Cooper Basin.|||Includes Arrabury and Tinchoo Formations.|Overlies Gidgealpa Group unconformably (?) and Toolachee Formation conformably.||
13823|Nappamerri Group|65925|5|Briefly described|p16 Fig.2.3, Appendix 2.|Triassic|Triassic|Cooper Basin.|||||Red beds; mudstone; siltstone; sandstone; lithic sandstone.|
13823|Nappamerri Group|66529|6|Mentioned|p12 Fig.5|||Eromanga Basin.||||Is unconformably overlain by Poolowanna Formation.||
13823|Nappamerri Group|67402|6|Mentioned|p90, p90 fig CPR4, p95|Middle Triassic|Late Permian|See also p96, p98, p100, p105.|||Includes the Arrabury Formation and Tinchoo Formation.|Overlies the Gidgealpa Group.||
13823|Nappamerri Group|68731|5|Briefly described|p200 Fig 3.110, p204, p205, p207|Middle Triassic|Lopingian|Nomenclatural history and subdivision of this group is outlined by Gray and McKellar (2002). Introduced by Papalia (1969, p.108). Raised to Group status by Powis (1989). Thickest in the Windorah and Arrabury troughs.|||Includes the Tinchoo Formation and Arrabury Formation (basal).|Unconformably overlain by the Poolawanna Formation and Hutton Sandstone or the Cuddapan Formation.|Contains distinct redbed characteristics.|17-JUL-14
13823|Nappamerri Group|69019|5|Briefly described|p82.|Middle Triassic|Permian|Southern Cooper Basin.|||||Dominated by fluvial sands.|
13823|Nappamerri Group|69023|5|Briefly described|p81-82, p151|Middle Triassic|Permian|Cooper Basin. Eroded by Middle Triassic tectonic activity causing tilting to the NE. Rocks of this unit are not known in the CALLABONNA sheet area.||||Conformably overlies Gidgealpa Group.||
13823|Nappamerri Group|69454|5|Briefly described|p38:4|Ladinian|Changhsingian|Cooper Basin.|||Arrabury, Tinchoo Formations.|Overlies Gidgealpa Group.||12-JUL-16
13823|Nappamerri Group|69673|6|Mentioned|p153 fig 125||||||Includes Arrabury Formation, Tinchoo Formation|||
13823|Nappamerri Group|69728|6|Mentioned|p285|Late Triassic|Permian|Cooper Basin.|||Arrabury, Tinchoo Formations.|||
13823|Nappamerri Group|69797|5|Briefly described|p17 Fig.2, p18|Middle Triassic|Early Triassic|Geol. Prov: Cooper Basin.|||Tinchoo Formation, Arrabury Formation|||
13823|Nappamerri Group|69946|5|Briefly described|p9, p52, p54|Late Triassic|Permian|Cooper Basin.|||Includes Arrabury and Tinchoo Formations.|Conformably overlies Gidgealpa Group. Is overlain unconformably by Cuddapan Formation.||
13823|Nappamerri Group|69947|5|Briefly described|p13 Fig.7.2, p16-17 Figs.7.5-6|Middle Triassic|Late Carboniferous|See also p21 Fig.7.10. Cooper Basin.|||Arrabury, Tinchoo Formations.|Overlies Gidgealpa Group. Is overlain unconformably by Cuddapan Formation.||
13823|Nappamerri Group|69948|6|Mentioned|p3-4|Early Triassic|Permian|Cooper Basin. Basement to Eromanga Basin in the southern Cooper region.||||||
13823|Nappamerri Group|70317|6|Mentioned|p33|Middle Triassic|Late Permian|Cooper Basin.|||Arrabury, Tinchoo Formations.|Overlies Gidgealpa Group. Is overlain unconformably by Cuddapan Formation.||
13823|Nappamerri Group|70823|4|Described|iv, p14, p25-p27|Middle Triassic|Lower Triassic|Cooper Basin. Seismic reflection and outcrop characteristics briefly discussed. This group has an average thickness of ~200m and is thickest in the Nappamerri Trough. This group is generally regarded as sealing the Gidgealpa Group. See also p39, p41, p49-p50, p70, p75-p77, p82.|||Includes the Arrabury Formation and the Tinchoo Formation.|Conformably overlies the Gidgealpa Group.||
13823|Nappamerri Group|70824|4|Described|p1, p5, p8, p37, p104-p107, p113, p123|Middle Triassic|Lower Triassic|Cooper Basin. Typically deposited as organically lean fluvial deposits. Areal extent and source rock geochemistry is discussed. This group reaches a maximum thickness close to 600m in the Nappamerri, Patchawarra and Arrabury troughs.|||Includes the Arrabury Formation and the Tinchoo Formation.|||
13823|Nappamerri Group|70946|5|Briefly described|p1087, p1089|Middle Triassic|Late Permian|Cooper Basin.|||Arrabury, Tinchoo Formations.|||08-OCT-18
13823|Nappamerri Group|71265|5|Briefly described|p589|Induan|Olenekian|Cooper Basin.|||Arrabury Formation.|Overlies Gidgealpa Group.||
13823|Nappamerri Group|71321|6|Mentioned|p15|||Of Patchawarra and Nappamerri troughs, Cooper Basin.||||||
13823|Nappamerri Group|71342|5|Briefly described|Ch4 p3-p4, Ch5 p9,  Ch5 p30|Early Triassic|Late Permian|Cooper Basin. See also Ch5 p52, Ch7 p13, Ch7 p16, Ch7 p21, Ch10 tbl 10.1, Ch10 p14, Ch10 p17, Ch10 p19-p20, Ch13 p7.|||Includes the Arrabury Formation and the Tinchoo Formation.|Overlies the Toolachee Formation. Unconformably overlain by the Hutton Sandstone.||
13823|Nappamerri Group|71701|5|Briefly described|p155|Olenekian|Induan|Cooper Basin.|||Includes the Arrabury Formation.|Overlies the Gidgealpa Group.||
13823|Nappamerri Group|72297|5|Briefly described|p742|||Cooper Basin. Has gas reservoirs at Marama and at Epsilon.||||||
13823|Nappamerri Group|72298|5|Briefly described|p801|Triassic||Eromanga Basin (SA,QLD).||||Is overlain unconformably by Poolowanna FZ.||
13823|Nappamerri Group|73167|5|Briefly described|p662, p664|Triassic|Triassic|Cooper Basin. Up to 500m of Nappamerri Group sediments uplifted and eroded along pre-existing faults in the Late Triassic E-W-compressional Hunter-Bowen Event, regional unconformity. Constituent units in Fig. 2, p664 confirmed in ASUD.|||Callamurra Member, Panning Member, Wimma Sandstone Member, Tinchoo Formation|Overlies the Toolachee Formation.|Floodplain, lacustrine and fluvial channel sediments.|
13823|Nappamerri Group|73244|6|Mentioned|p86|Triassic|Triassic|Cooper Basin. Floodplain, lacustrine, fluvial channels.||||||
13823|Nappamerri Group|73251|6|Mentioned|p62|Middle Triassic|Permian|Cooper Basin. Non-marine depositional environments.|||Tinchoo Formation, Arrabury Formation, Wimma Sandstone Member, Paning Member, Callamurra Member|Underlain by Toolachee Formation (Gidgealpa Group).||
13823|Nappamerri Group|73343|5|Briefly described|p337-338|Triassic|Triassic|Cooper Basin. Reflects floodplain, lacustrine, and fluvial channel settings. Incised during the Late Triassic Hunter-Bowen Event.|||Tinchoo Formation, Wimma Sandstone Member, Panning Member, Callamurra Member|Underlain by Toolachee Formation.||
13823|Nappamerri Group|73479|5|Briefly described|p156 Fig.2, p159, p163, p166|Triassic|Triassic|Cooper Basin. Floodplain, lacustrine, fluvial channels depositional environment. Highly efficient regional seal. Up to 500 m thickness was exhumed and eroded in Hunter-Bowen Event.|||Callamurra Member, Panning Member, Wiumma Sandstone Member, Tinchoo Formation|Overlies Toolachee Formation, unconformably underlies Cuddapan Formation||
13823|Nappamerri Group|73495|6|Mentioned|p498|Middle Triassic|Lower Triassic|Cooper Basin. Up to 550 m thick.||||||
13841|Naracoorte Limestone Member|22587|6|Mentioned|p79 Fig. 7|Early Miocene||Of Gambier Limestone, Heytesbury Group.||||||
13841|Naracoorte Limestone Member|22626|6|Mentioned|446 fig 10|Middle Miocene|Early Miocene|Geol province West Otway Basin.||||||
13841|Naracoorte Limestone Member|23322|5|Briefly described|957 Fig.2|Middle Miocene|Early Miocene|Of the Gambier Limestone.  Geological Province: Gambier Basin.  See also p967.||||||07-SEP-09
13841|Naracoorte Limestone Member|32116|6|Mentioned|p45|||Stratigraphy||||||
13841|Naracoorte Limestone Member|39077|6|Mentioned|p32|||||||||
13841|Naracoorte Limestone Member|42594|5|Briefly described|P 247|||early-mid Miocene||||||
13841|Naracoorte Limestone Member|42966|2|Defined|Table 16, p127|Early Miocene||of Gambier Limestone||||||
13841|Naracoorte Limestone Member|43195|5|Briefly described|Map Legend|Middle Miocene|Late Eocene|see also commentary on back of map. Of Heytesbury Group.||||||
13841|Naracoorte Limestone Member|43814|6|Mentioned|Fig.3,p115|||||||||
13841|Naracoorte Limestone Member|44133|5|Briefly described|p156|Early Miocene|Early Miocene|Of the Gambier Limestone (Heytesbury Group). Geological Province: Gambier Basin. Thickness: 6m.||||||
13841|Naracoorte Limestone Member|63124|3|Fully described|p87 Fig. 5.29, p93|Early Miocene|Early Miocene|Of Gambier Limestone. Unconformably overlain at type section by 'aeolinite', probably Bridgewater Formation. Age: ~19Ma. Thickness: 6m. Geol.Prov: Gambier Basin. Lateral equiv.of Crayfish Member. May grade laterally into Mannum Limestone (Murray Basin).||||||31-JAN-08
13841|Naracoorte Limestone Member|69297|5|Briefly described|p79|Serravallian|Burdigalian|Otway Basin.||Gambier Limestone||Overlies the Green Point Member. Unconformably overlain by the Coomandook Formation.|Limestones.|
13841|Naracoorte Limestone Member|70077|5|Briefly described|Nelson: Fig.2. Regional: Fig.4|Miocene|Miocene|Otway Basin: Gambier Embayment and Voluta Trough.||Gambier Limestone.||Overlies Green Point Member. Is overlain by Coomandook Formation.||
13841|Naracoorte Limestone Member|70078|5|Briefly described|Northern: Fig.2. Regional: Fig.4|Miocene|Miocene|Gambier Embayment and Voluta Trough.||Gambier Limestone.||Overlies Green Point Member. Is overlain by Coomandook Formation.||
13858|Narina Greywacke|22766|5|Briefly described|Fig.2 p561, p561|Early Cambrian|Early Cambrian|||||||
13858|Narina Greywacke|23818|5|Briefly described|p87 Fig.33, p91|Cambrian|Cambrian|Top unit of the Hawker Group. Max. thickness: 4500 ft.||||||
13858|Narina Greywacke|23981|5|Briefly described|o8-9 Fig. 4, p10 Fig. 5|Early Cambrian|Early Cambrian|Overlies Oparinna Shale; underlies Billy Creek Formation. Geological Province: Arrowie Basin.||||||
13858|Narina Greywacke|24176|4|Described|p23 Tb. 1, p17|Cambrian|Cambrian|Gritty green sandstone, cream and purple dolomites.  Overlies and intertongues with Oraparinna Shale.  Max. thickness: >700m.  Geological Province: Mount Painter Province.||||||
13858|Narina Greywacke|24465|5|Briefly described|p345 Fig.2|Early Cambrian|Early Cambrian|Of the Hawker Group.  Geological Province: Arrowie Basin.||||||19-JAN-05
13858|Narina Greywacke|29929|6|Mentioned|Fig.1|||||||||
13858|Narina Greywacke|30176|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
13858|Narina Greywacke|30801|6|Mentioned|p5|||Hawker Group. Table P5-6.||||||
13858|Narina Greywacke|30802|5|Briefly described|p11|||Cambrian age||||||
13858|Narina Greywacke|30807|6|Mentioned|p102|||Suggested map symbol||||||
13858|Narina Greywacke|33474|6|Mentioned|Fig.3|||||||||
13858|Narina Greywacke|33932|4|Described|p18|||||||||
13858|Narina Greywacke|33934|4|Described|Fig.2|||L.Camb.||||||
13858|Narina Greywacke|34185|6|Mentioned|p129|||||||||
13858|Narina Greywacke|34269|6|Mentioned|Table 1|||||||||
13858|Narina Greywacke|34612|5|Briefly described|p91|||Correlation chart. Fig.33. Cambrian||||||
13858|Narina Greywacke|35255|6|Mentioned|Fig.8|||||||||
13858|Narina Greywacke|36198|6|Mentioned|Fig.I.2|||||||||
13858|Narina Greywacke|38068|6|Mentioned|p69|||||||||
13858|Narina Greywacke|40852|6|Mentioned|Fig.3.|||||||||
13858|Narina Greywacke|42011|6|Mentioned|Fig.3 P458|||||||||
13858|Narina Greywacke|42222|6|Mentioned|Table 1 P5|||||||||
13858|Narina Greywacke|42225|6|Mentioned|Fig.4 P224|||||||||
13858|Narina Greywacke|42272|6|Mentioned|p414|||||||||
13858|Narina Greywacke|42440|6|Mentioned|Fig.2 P602|||||||||
13858|Narina Greywacke|42458|5|Briefly described|Fig.2 P699|||||||||
13858|Narina Greywacke|43759|6|Mentioned|p452|||||||||
13858|Narina Greywacke|44133|5|Briefly described|p4 Fig. 7.2, 25, 26|Early Cambrian|Early Cambrian|Geological Province: Arrowie Basin. Maximum Thickness: 540m. Intertounges with Oraparinna Shale.||||||
13858|Narina Greywacke|60418|5|Briefly described|p135|Early Cambrian|Early Cambrian|Of the Hawker Group. Geological Province: Arrowie Basin of Adelaide Geosyncline.||||||18-MAY-05
13858|Narina Greywacke|60889|4|Described|p249|Early Cambrian|Early Cambrian|||Hawker Group||Intertongues with Oraparinna Shale.|Succession of silty to medium-grained feldspathic sandstone.|21-SEP-17
13858|Narina Greywacke|60959|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of the Hawker Group. Khaki-green, flat to ripple laminated, silty to medium grained feldspathic sandstone.||||||
13858|Narina Greywacke|60990|5|Briefly described|p83 Fig.2 |Botoman|Botoman|Flinders Ranges.||Hawker Group.||||
13858|Narina Greywacke|63447|5|Briefly described|p962,p963 Fig.2|Early Cambrian|Early Cambrian|||Hawker Group||Overlain by Billy Creek Formation. Part lateral equivalent to Oraparinna Shale, Upper Wilkawillina Limestone.||
13858|Narina Greywacke|63569|6|Mentioned|p117 Fig.1|Early Cambrian|Early Cambrian|Arrowie Basin.||||||
13858|Narina Greywacke|65375|5|Briefly described|p33.|Early Cambrian|Early Cambrian|||Unit in Hawker Group.||Overlies Oraparinna Shale. Is overlain by Billy Creek Formation.||
13858|Narina Greywacke|65892|5|Briefly described|p9 Fig.4, p10.|Early Cambrian|Early Cambrian|Arrowie Basin. In eastern Nepabunna Trough, intertongues with Oraparinna Shale.||Unit in Hawker Group.|||Fine- to medium-grained feldspathic sandstone.|
13858|Narina Greywacke|65925|6|Mentioned|p14 Fig.2.2.|Early Cambrian|Early Cambrian|||||||
13858|Narina Greywacke|68735|5|Briefly described|p233 Fig.2, p234, p235 Fig.3|Early Cambrian|Early Cambrian|Arrowie Basin.||Of the Hawker Group.||Underlain by the Oraparinna Shale.|Comprises silty feldspathic sandstones.|
13858|Narina Greywacke|68993|6|Mentioned|p544 Fig.1|Early Cambrian|Early Cambrian|Arrowie Basin.||Of the Hawker Group.||||
13858|Narina Greywacke|69570|6|Mentioned|p421 fig 1|Cambrian|Cambrian|Arrowie Syncline, Flinder Ranges.||||||
13858|Narina Greywacke|72429|6|Mentioned|p975||||||||Includes coarse gritty sandstones.|
13904|Narrawaturk Marl|12781|6|Mentioned|p386|Eocene|Eocene|Otway Basin. Maximum thickness 21m.||Nirranda Group.||Unconformably overlies Dilwyn Formation. Is overlain unconformably by Compton Conglomerate and Gellibrand Marl.||
13904|Narrawaturk Marl|22587|6|Mentioned|p79 Fig.7|Late Eocene|Middle Eocene|||||||
13904|Narrawaturk Marl|22674|5|Briefly described|Fig.2 p719|Early Oligocene|Middle Eocene|||||||
13904|Narrawaturk Marl|22875|3|Fully described|p62|Early Oligocene|Late Eocene|Of the Nirranda Group.||||||31-JAN-07
13904|Narrawaturk Marl|22944|5|Briefly described|Fig3|Oligocene|Eocene|||||||
13904|Narrawaturk Marl|23230|5|Briefly described|Table4-1p40|Oligocene||||||||
13904|Narrawaturk Marl|23307|5|Briefly described|Map Legend|Oligocene|Eocene|Of Nirranda Group.||||||31-JAN-07
13904|Narrawaturk Marl|23322|5|Briefly described|957 Fig.2|Oligocene|Eocene|Of the Nirranda Group.  Geological Province: Gambier Basin.  See also p968.||||||07-SEP-09
13904|Narrawaturk Marl|24056|5|Briefly described|p85|Eocene|Eocene|Of Nirranda Group.  Geological Basin: Otway Basin.||||||
13904|Narrawaturk Marl|24202|5|Briefly described|p313 Fig. 2|Late Eocene|Middle Eocene|Geological Province: Gambier Sub-basin.||||||
13904|Narrawaturk Marl|24314|5|Briefly described|p61 Fig.2|Eocene|Eocene|Of the Nirranda Group. Geological Province: Otway Basin. Max. Thickness 21m.||||||09-DEC-08
13904|Narrawaturk Marl|24551|5|Briefly described|p292 Fig. 10.3|||||||||
13904|Narrawaturk Marl|24562|5|Briefly described|p7, 8 Fig. 2|Oligocene|Eocene|Of the Nirranda Group. Conformably overlies Mepunga Formation.  Geological Province: Otway Basin.||||||09-DEC-08
13904|Narrawaturk Marl|29823|6|Mentioned|p14|||||||||
13904|Narrawaturk Marl|30576|5|Briefly described|Table 2|||||||||
13904|Narrawaturk Marl|30578|6|Mentioned|p9|||||||||
13904|Narrawaturk Marl|30580|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
13904|Narrawaturk Marl|30675|5|Briefly described|p253|||Lithology and radioactivity.||||||31-JAN-07
13904|Narrawaturk Marl|30932|6|Mentioned|Map legend|Miocene|Oligocene|Part of Gellibrand Marl? Oligocene to Miocene||||||31-JAN-07
13904|Narrawaturk Marl|31036|6|Mentioned|p210|||Unit of Nirranda Gp. See also Table 9-1.||||||
13904|Narrawaturk Marl|31245|6|Mentioned|p82|||||||||
13904|Narrawaturk Marl|31424|4|Described|p14|||See also p7. Described from core.||||||31-JAN-07
13904|Narrawaturk Marl|31625|6|Mentioned|Fig. 5.2|||Eocene-Oligocene||||||
13904|Narrawaturk Marl|32852|6|Mentioned|p10|||||||||
13904|Narrawaturk Marl|33155|5|Briefly described|p122|||||||||
13904|Narrawaturk Marl|33940|6|Mentioned|p414|||||||||
13904|Narrawaturk Marl|34063|6|Mentioned|p2|||U.Eocene. Table||||||
13904|Narrawaturk Marl|34954|6|Mentioned|Fig.35|||||||||
13904|Narrawaturk Marl|35066|5|Briefly described|p209|||||||||
13904|Narrawaturk Marl|36913|6|Mentioned|Fig.2|||||||||
13904|Narrawaturk Marl|37548|6|Mentioned|Fig.5|||||||||
13904|Narrawaturk Marl|38625|6|Mentioned|Table 2|||||||||
13904|Narrawaturk Marl|38932|5|Briefly described|p98|||See also Fig.4||||||
13904|Narrawaturk Marl|40003|5|Briefly described|p44|||||||||
13904|Narrawaturk Marl|40560|6|Mentioned|p6|||||||||
13904|Narrawaturk Marl|41016|5|Briefly described|Table 1|||||||||
13904|Narrawaturk Marl|41185|6|Mentioned|Fig.4|||||||||
13904|Narrawaturk Marl|41269|5|Briefly described|p246|||||||||
13904|Narrawaturk Marl|41517|6|Mentioned|p135|||See also p139.||||||31-JAN-07
13904|Narrawaturk Marl|41642|6|Mentioned|Fig.8.6|||||||||
13904|Narrawaturk Marl|41701|6|Mentioned|Map legend|Oligocene||||||||
13904|Narrawaturk Marl|41704|6|Mentioned|Fig.3|||||||||
13904|Narrawaturk Marl|41714|6|Mentioned|Fig.2|||||||||
13904|Narrawaturk Marl|41726|6|Mentioned|Fig.5|||||||||
13904|Narrawaturk Marl|41769|4|Described|p30|||||||||
13904|Narrawaturk Marl|41868|5|Briefly described|p535|||||||||
13904|Narrawaturk Marl|42318|6|Mentioned|Fig.2 P10|||||||||
13904|Narrawaturk Marl|42524|5|Briefly described|Fig.3 P27|||||||||
13904|Narrawaturk Marl|42601|6|Mentioned|Fig.2 p15|||||||||
13904|Narrawaturk Marl|42827|5|Briefly described|p283|||see also Fig 12.30||||||
13904|Narrawaturk Marl|42863|5|Briefly described|Fig.14|||Variation on Victorian unit.||||||
13904|Narrawaturk Marl|43171|6|Mentioned|5-8|||Of Nirranda Group. Age: 30-40Ma.||||||31-JAN-07
13904|Narrawaturk Marl|43195|5|Briefly described|Map Legend||Late Eocene|See also commentary on back of map. Of Nirranda Group.||||||
13904|Narrawaturk Marl|43208|5|Briefly described|map legend|Early Oligocene|Middle Eocene|Of Nirranda Group.||||||
13904|Narrawaturk Marl|43219|5|Briefly described|Fig.3,p6.|Oligocene|Eocene|Of the Nirranda Group.||||||31-JAN-07
13904|Narrawaturk Marl|43590|4|Described|p22|Early Oligocene|Late Eocene|||||||
13904|Narrawaturk Marl|43660|6|Mentioned|Fig.6,p15|Oligocene|Eocene|||||||
13904|Narrawaturk Marl|43733|6|Mentioned|Fig.2.11,p65||Eocene|||||||
13904|Narrawaturk Marl|43744|6|Mentioned|Fig.3,p3|||||||||
13904|Narrawaturk Marl|43814|6|Mentioned|Fig.3,p115|||||||||
13904|Narrawaturk Marl|43937|5|Briefly described|Map Legend|Middle Eocene|Paleocene|||||||
13904|Narrawaturk Marl|44133|5|Briefly described|p155|Early Oligocene|Middle Eocene|Of the Nirranda Group. Geological Province: Gambier Basin. Thickness: 15m. Conformably overlies: Mepunga Formation.||||||
13904|Narrawaturk Marl|48911|6|Mentioned|Chart 1|||||||||
13904|Narrawaturk Marl|60563|5|Briefly described|p47|||Of the Nirranda Group. See also the Narrawaturk Formation.||||||
13904|Narrawaturk Marl|61155|5|Briefly described|p18|Early Oligocene|Middle Eocene|Of the Nirranda Group. Partly overlies and interfingers with Mepunga Formation. Underlies Clifton Formation. Age: 48-30.5Ma. Thickness: 130m. Geological Province: Otway Basin (Tyrendarra and Port Campbell Embayments).||||||
13904|Narrawaturk Marl|61182|3|Fully described|p24, p26, p33|Oligocene|Eocene|Of Nirranda Gp. Incorporates Browns Creek Clay, Castle Cove Limest., Glen Aire Clay.Grades into/conformable over Mepunga Fm; interfingers with Demons Bluff Fm. Max.thick: 131m. Disconformable below Clifton Fm; and Gellibrand Marl in places. Fossils common||||||
13904|Narrawaturk Marl|61547|6|Mentioned|p461 Fig.2. |Eocene|Eocene|||Unit in Nirranda Group.||Overlies Mepunga Formation. Is overlain by Gellibrand Marl.||
13904|Narrawaturk Marl|61622|5|Briefly described|p436 Fig. 2|Eocene|Eocene|Of Nirranda Group. Geological Province: Otway Basin.||||||07-FEB-11
13904|Narrawaturk Marl|61623|6|Mentioned|p449 Fig. 4|Oligocene|Eocene|Of Nirranda Group. Geological Province: Otway Basin.||||||07-APR-09
13904|Narrawaturk Marl|61624|6|Mentioned|p466 Fig. 2|Oligocene|Eocene|Of Nirranda Group. Geological Province: Otway Basin.||||||07-APR-09
13904|Narrawaturk Marl|61626|5|Briefly described|p486, p486 Fig. 2, p488 Fig. 4|Oligocene|Eocene|Of Nirranda Group. Geological Province: Otway Basin.||||||07-APR-09
13904|Narrawaturk Marl|61627|5|Briefly described|p504, p500 Fig. 2|Late Eocene|Middle Eocene|Of Nirranda Group. Underlain by Mepunga Sandstone. Geological Province: Otway Basin.||||||07-FEB-11
13904|Narrawaturk Marl|61628|5|Briefly described|p509 Fig. 3|Early Oligocene|Middle Eocene|Of Nirranda Group. Geological Province: Otway Basin.||||||07-APR-09
13904|Narrawaturk Marl|63122|5|Briefly described|p17 Fig. 4.3|Late Eocene|Middle Eocene|Of the Nirranda Group. Max. thickness: 21m. Geological Province: Otway Basin.||||||
13904|Narrawaturk Marl|63124|3|Fully described|p49 Fig. 5.2, p87 Fig. 5.29, p91|Late Eocene|Middle Eocene|Of Nirranda Gp. Conformable on Mepunga Fm; unconformable on Dilwyn Fm. Conformable below Greenways Mbr (Gambier Lst) or unconformable below Camelback Mbr. Age: ~39.5-~36.5Ma). Max.thickness:21m. In Otway Basin. Synonym: Lacepede Formation (Ludbrook 1971).||||||31-JAN-08
13904|Narrawaturk Marl|63129|6|Mentioned|p139|||Geological Province: Otway Basin. Acts as a regional seal.||||||30-JAN-08
13904|Narrawaturk Marl|63130|5|Briefly described|p146|Tertiary|Tertiary|Overlies Dilwyn Formation. Geological Province: Otway Basin.||||||06-FEB-08
13904|Narrawaturk Marl|63269|5|Briefly described|p605|Oligocene|Eocene|Otway Basin.||Nirranda Group.||||
13904|Narrawaturk Marl|63431|5|Briefly described|p677 Fig. 2|Eocene|Eocene|Of the Nirranda Group. Geological Province: Penola Trough/Otway Basin.||||||07-FEB-11
13904|Narrawaturk Marl|65715|5|Briefly described|p11 Tb.7, p25 Fig.1a|Paleogene|Paleogene|Of Nirranda Group. Formation status.||||||
13904|Narrawaturk Marl|66002|4|Described|p10 Tb.7, p16, p26 Fig.7|Paleogene|Paleogene|Of Nirranda Group. Overlies Mepunga Formation. Calcareous mudstone, minor thin calcarenite beds, locally carbonaceous and burrowed, locally abundant glauconite pellets, polished quartz sands. Contains foraminifers, bryozoans, brachiopods and molluscs. Defined by White 1968.||||||
13904|Narrawaturk Marl|66245|6|Mentioned|p6 Fig.5. |Rupelian|Bartonian|||Unit in Nirranda Group.||||
13904|Narrawaturk Marl|67061|6|Mentioned|p546 Fig.3.|Oligocene|Eocene|||Unit in Nirranda Group.||||
13904|Narrawaturk Marl|67366|5|Briefly described|p103 Fig.2. |Oligocene|Eocene|||Unit in Nirranda Group.||Overlies Mepunga Formation. Is unconformably overlain by Clifton Formation.|Open marine marl and calcareous mudstone.|
13904|Narrawaturk Marl|68116|5|Briefly described|Appendix, Maps 54-55.|Oligocene|Eocene||||||Calcareous mudstone, minor thin calcarenite beds: locally carbonaceous and burrowed, locally abundant glauconite pellets and polished quartz sand, foraminifers, bryozoans, brachiopods and molluscs; open marine (below storm wave base) deposits.|
13904|Narrawaturk Marl|69297|5|Briefly described|p79|Rupelian|Bartonian|Otway Basin.||Nirranda Group||Overlies the Mepunga Formation. Overlain by the Gambier Limestone and the Wangoom Sand or unconformably by the Clifton Formation.|Marl.|
13904|Narrawaturk Marl|69651|5|Briefly described|p10|Oligocene|Eocene|||Nirranda Group.||Overlies Mepunga Formation. Is overlain unconformably by Clifton Formation.||
13904|Narrawaturk Marl|70077|5|Briefly described|Nelson: Fig.2. Regional: Fig.4; p5|Eocene|Eocene|Otway Basin. Increasingly open marine carbonates. Time-equivalent to Demons Bluff Formation and Eastern View Coal Measures.||Nirranda Group.||Overlies Mepunga Formation. Is overlain by Clifton Formation or Greenways Member (Gambier Limestone). Is locally interbedded with Wangoom Sand.||
13904|Narrawaturk Marl|70078|5|Briefly described|Northern: Fig.2. Regional: Fig.4|Eocene|Eocene|Gambier Embayment and Voluta Trough.||Nirranda Group.||Overlies Mepunga Formation. Is overlain by Gambier Limestone.||
13904|Narrawaturk Marl|70880|6|Mentioned|p77|Oligocene|Eocene|Otway Basin.||||||
13904|Narrawaturk Marl|70942|4|Described|p126, 119|||||||||17-FEB-17
13904|Narrawaturk Marl|71266|6|Mentioned|p614 Fig.3|Oligocene|Eocene|Otway Basin.||||||
13904|Narrawaturk Marl|71437|4|Described|Fig. 1 opp 154, p155, p160|Oligocene|Eocene|||Of Nirranda Group.||Interfingers with Mepunga Formation. Succeeded partially disconformably by Clifton Formation.|Sequence of richly fossiliferous marls, grading down in carbonate content to marly mudstones, or up to marly limestones.|
13904|Narrawaturk Marl|73357|5|Briefly described|p28-30, p44, p46, p48|Rupelian|Priabonian|Otway Basin. Contains Nothofagidites asperus Spore-Pollen Zone, Proteacidites tuberculatus Spore-Pollen Zone, Spiniferites ramosus Dinocyst Zone and Operculodinium Dinocyst Superzone, typically nearshore to offshore marine depositional environments. Lower part correlated with Corrudinium incompositum Dinocyst Zone.||Of Nirranda Group|Includes Wangoom Sand Member|Overlies Mepunga Formation, underlies Clifton Formation.||
13904|Narrawaturk Marl|73383|5|Briefly described|p3, p10 Tb.3.8, p25, p28, p164-165, p258|Oligocene|Eocene|Otway Basin. Approximately equivalent to chemostratigraphic package S6-P1 which has high Fe/Al values, the top of the package is defined by a decrease in Ti/Cr values and an increase in Ca. Lithologies based on geochemistry using the ChemLith classification includes calcareous sandstone and calcareous limestone, and using the Herron classification (1988) includes Fe-sand, Fe-shale and quartz-arenite. See also vi, p11 Tb.3.9, p34, p131.||Nirranda Group||Overlies Mepunga Formation, underlies Heytesbury Group, Gellibrand Marl|Marls and calcareous mudstones.|
13904|Narrawaturk Marl|73385|5|Briefly described|p5|Oligocene|Eocene|Otway Basin.||Nirranda Group||Overlies Mepunga Formation, underlies Gellibrand Marl, Clifton Formation.|Open marine marls and calcareous mudstones.|
13904|Narrawaturk Marl|73386|4|Described|p4, p6, p13, Attachment A1|Rupelian|Priabonian|Otway Basin. Widespread unit. Open marine depositional environment. Belongs to the Middle Nothofagidites asperus to Lower Proteacidites tuberculatus spore-pollen subzones, latest Priabonian to Rupelian in age.||Nirranda Group||Overlies Mepunga Formation, underlies Clifton Formation, Gellibrand Marl, Heytesbury Group|Marls and calcareous mudstones.|
13904|Narrawaturk Marl|73486|6|Mentioned|p511 Fig.2|Rupelian|Bartonian|Otway Basin.||Nirranda Group||||
13904|Narrawaturk Marl|73594|5|Briefly described|p4|Oligocene|Eocene|Otway Basin.||Nirranda Group||Overlies Mepunga Formation|Marine marls and calcareous mudstones.|
13978|Nelson Bay Formation|24551|5|Briefly described|p338 Fig. 11.2, 342|Early Pleistocene|Early Pleistocene|Maximum Thickness:>30m.  Age 1.0-1.4 Ma, from Figure 11.2, p 338.|1.0 - 1.4 Ma||||Subhorizontal biocalcarenite, lagoonal sediments and paleosols|20-JUN-12
13978|Nelson Bay Formation|33160|6|Mentioned|p301|||See also P304||||||
13978|Nelson Bay Formation|34988|3|Fully described|p290|||||||||
13978|Nelson Bay Formation|40643|5|Briefly described|p145|||||||||
13978|Nelson Bay Formation|41206|6|Mentioned|p365|||||||||
13978|Nelson Bay Formation|41848|3|Fully described|p365|||Overlain by Bridgewater Formation Probably early Pleistocene. Shown as Nelson Formation on p366||||||
13978|Nelson Bay Formation|42827|6|Mentioned|p373|||||||||
13978|Nelson Bay Formation|44133|5|Briefly described|p222|||Underlies: Bridgewater Formation.||||||
13978|Nelson Bay Formation|44221|14|Not recorded|p.95|||||||||
13978|Nelson Bay Formation|50079|6|Mentioned|p46|||Lacustrine sediments largely of nearby Portland Limestone which was levelled and redeposited; calcarenite beds interspersed with clay beds.||||||
13978|Nelson Bay Formation|62068|5|Briefly described|p135 Fig.2,p135,p136,p138,|Pleistocene|Pleistocene|Said to have a Lower Member where fossil vertebrate material collected, mostly from Unit B (of Hann, 1983). Dated by magnetic polarity stratigraphy. Constrained to the Matuyama Chron (1.77-0.78 Ma) by foraminiferan Globorotalia truncatulinoides (F.A.D. 1.9 Ma) and K-Ar dates of 2.76 and 3.20 Ma for the underlying basalts (McFadden et al. 1987)||||Unconformably overlies a basalt of the Newer Volcanics. Unconformably overlain by the Bridgewater Formation.|Series of horizontal and cross-bedded calcarenite, clay and sand.|
14004|Nepabunna Siltstone|22766|6|Mentioned|p567|||||||||
14004|Nepabunna Siltstone|23981|5|Briefly described|p8-9 Fig. 4, p10 Fig. 5|Early Cambrian|Early Cambrian|Geological Province: Arrowie Basin.||||||15-FEB-07
14004|Nepabunna Siltstone|24176|5|Briefly described|p17, p23 Tb. 1|Cambrian|Cambrian|Dark blue calcareous siltstone.  Max. thickness: 490m.  Geological Province: Mount Painter Province.||||||
14004|Nepabunna Siltstone|30176|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
14004|Nepabunna Siltstone|30801|6|Mentioned|p5|||Lower Cambrian. Table P5-6||||||
14004|Nepabunna Siltstone|30807|6|Mentioned|p102|||Suggested map symbol||||||
14004|Nepabunna Siltstone|31797|6|Mentioned|Fig. 2|||L.Cambrian. Hawker Gp.||||||
14004|Nepabunna Siltstone|35255|6|Mentioned|Fig.8|||||||||
14004|Nepabunna Siltstone|42011|6|Mentioned|Fig.3 P458|||||||||
14004|Nepabunna Siltstone|42225|6|Mentioned|Fig.4 P224|||||||||
14004|Nepabunna Siltstone|42272|6|Mentioned|p414|||||||||
14004|Nepabunna Siltstone|42440|6|Mentioned|Fig.2 P602|||||||||
14004|Nepabunna Siltstone|44133|5|Briefly described|p4 Fig. 7.2, 23|Early Cambrian|Early Cambrian|Geological Province: Arrowie Basin. Intertounges with Mernmerna Formation.||||||
14004|Nepabunna Siltstone|60418|5|Briefly described|p135|Early Cambrian|Early Cambrian|Of the Hawker Group. Geological Province: Arrowie Basin of Adelaide Geosyncline.||||||
14004|Nepabunna Siltstone|60889|4|Described|p247 Fig.4, p248, p251|Early Cambrian|Early Cambrian|North-Central Trough, Arrowie Basin.||Hawker Group||Intertongues with Mernmerna Formation.|Siltstone.|21-SEP-17
14004|Nepabunna Siltstone|63447|6|Mentioned|p963 Fig.2 |Early Cambrian|Early Cambrian|||||Shown as lateral equivalent to upper Wilkawillina Limestone in part, Bendieuta Formation, Midwerta Shale, Mernmerna Formation (Parara Limestone) in part.||
14004|Nepabunna Siltstone|63569|6|Mentioned|p117 Fig.1|Early Cambrian|Early Cambrian|Arrowie Basin.||||||
14004|Nepabunna Siltstone|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.||||
14004|Nepabunna Siltstone|65925|6|Mentioned|p14 Fig.2.2.|Early Cambrian|Early Cambrian|||||||
14004|Nepabunna Siltstone|68735|5|Briefly described|p234, p235 Fig.3|Early Cambrian|Early Cambrian|Arrowie Basin.||Hawker Group.||Interfingers with the Mernmerna Formation.|Fine-grained clastic unit.|10-APR-17
14004|Nepabunna Siltstone|68993|6|Mentioned|p544 Fig.1|Early Cambrian|Early Cambrian|Arrowie Basin.||Of the Hawker Group.||||
14004|Nepabunna Siltstone|69570|6|Mentioned|p421 fig 1|Cambrian|Cambrian|Arrowie Syncline, Flinder Ranges.||||||
14004|Nepabunna Siltstone|70833|6|Mentioned|p181|Cambrian|Cambrian|Of Arrowie Basin. Key section: MOG (S of Moro Gorge, Arrowie Syncline),||||||
14004|Nepabunna Siltstone|71102|5|Briefly described|p242,247,249,251|||Of Arrowie Basin. Intersected section: BHG (Bullock Head Gap, SW Arrowie Syncline)|||||Black, laminated, argillaceous, pyritic and manganiferous lime-shale.|
14121|Ngaltinga Formation|22525|4|Described|p37,38,40||Pleistocene|also called Ngaltinga Clay by Ward (1966)||||||
14121|Ngaltinga Formation|23489|4|Described|p46|Pleistocene|Pleistocene|Formerly Ngaltinga Clay.||||||
14121|Ngaltinga Formation|40450|6|Mentioned|p67|||||||||
14121|Ngaltinga Formation|41551|5|Briefly described|p465|||||||||
14121|Ngaltinga Formation|68811|5|Briefly described|p88|||Separates the Port Willunga Formation from the overlying Quaternary aquifer.||||Overlies the Port Willunga Formation.|Silty clay.|15-APR-20
14121|Ngaltinga Formation|70660|4|Described|p3, p9-p11|Middle Pleistocene|Middle Pleistocene|See also p20 fig 11a, p21 fig 11c, p29-p30, p40, p46.|||Includes the Snapper Point Sand Member.|Overlies the Ochre Cove Formation.|Grey-green or olive sandy clay.|
14121|Ngaltinga Formation|72450|6|Mentioned|Brochure, Brochure map|Quaternary|Quaternary|Up to 5m thick. Underlies the plains in southwestern part of the Willunga Embayment.||||Overlies the Pirramimma Sandstone.|Thick, grey-green and red-brown mottled clay.|
14121|Ngaltinga Formation|73188|5|Briefly described|p319-320, p335|Pleistocene|Pleistocene|St Vincent Basin.||||Equivalent to Keswick Clay. [Underlain by Ochre Cove Formation].|Smectite-rich clays characterised by gilgai structures.|
14133|Niggly Gap beds|42813|6|Mentioned|p15|||||||||
14133|Niggly Gap beds|65925|5|Briefly described|Appendix 2.||||||||Siltstone, micaceous; sandstone; dolomite.|
14133|Niggly Gap beds|73059|6|Mentioned|p1061|||Contains detrital zircons sourced from the adjacent Gawler Craton.||||||
14133|Niggly Gap beds|73264|6|Mentioned|p1386, p1387 Fig.10|||Adelaide Rift Complex. Major ziron peaks in the range 1400-1900 Ma, secondary peaks at 900-1250 Ma.||||||
14143|Nilpena Limestone|23818|5|Briefly described|p216 Fig.112|Middle Pleistocene|Middle Pleistocene|||||||
14143|Nilpena Limestone|24176|5|Briefly described|p20, p22 Tb. 1|Quaternary|Quaternary|Geological Province: Mount Painter Province.||||||
14143|Nilpena Limestone|29781|6|Mentioned|p51|||||||||
14143|Nilpena Limestone|30176|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
14143|Nilpena Limestone|30177|6|Mentioned|p106|||||||||
14143|Nilpena Limestone|30807|6|Mentioned|p101|||Suggested map symbol||||||
14143|Nilpena Limestone|34180|5|Briefly described|p216|||Middle Pleistocene. Equivalent? Bung Limestone.||||||
14143|Nilpena Limestone|34291|6|Mentioned|p32|||Quaternary. See also PP34,91||||||
14143|Nilpena Limestone|38068|6|Mentioned|p76|||||||||
14185|Nirranda Group|12781|6|Mentioned|p386|Eocene|Eocene|Otway Basin. Appears as NIRR. GP.|||Narrawaturk Mark.|Overlies Wangerip Group. Is overlain by Heytsbury Group.||
14185|Nirranda Group|22587|6|Mentioned|p79 Fig.7|Late Eocene|Middle Eocene|||||||
14185|Nirranda Group|22674|5|Briefly described|p718, Fig.2 p719|Early Oligocene|Middle Eocene|||||||
14185|Nirranda Group|22875|4|Described|p59|Early Oligocene|Middle Eocene|Age: 29-45Ma.||||||31-JAN-07
14185|Nirranda Group|22944|5|Briefly described|Fig3|Oligocene|Eocene|||||||
14185|Nirranda Group|23249|5|Briefly described|p143 Fig.2|Early Oligocene|Late Eocene|In the Otway Basin.||||||31-JAN-07
14185|Nirranda Group|23307|5|Briefly described|Map Legend|Oligocene|Eocene|||||||
14185|Nirranda Group|23322|5|Briefly described|957 Fig.2|Oligocene|Eocene|Geological Province: Gambier Basin (SA) and Otway Basin (VIC).||||||07-SEP-09
14185|Nirranda Group|23778|5|Briefly described|p660|||Geological Province: Otway Basin.||||||
14185|Nirranda Group|23792|5|Briefly described|p26|Recent|Eocene|Carbonates and siliciclastics. Geological Province: Otway Basin.||||||01-JUL-13
14185|Nirranda Group|23939|6|Mentioned|Fig.5|||May be Middle Eocene to Early Oligocene in age.||||||
14185|Nirranda Group|24056|5|Briefly described|p84, p85|||Geological Basin: Otway Basin.||||||
14185|Nirranda Group|24177|5|Briefly described|p14|Eocene|Eocene|Age: ~45 Ma. Geological Province: Otway Basin.||||||
14185|Nirranda Group|24200|5|Briefly described|p417|||See also p423 Figs. 15, 16, p428 Fig. 18.  Nirranda Group Equivalents discussed throughout text.||||||
14185|Nirranda Group|24314|5|Briefly described|p61 Fig.2|Eocene|Eocene|Geological Province: Otway Basin.||||||
14185|Nirranda Group|24323|5|Briefly described|p136 Fig. 3|Oligocene|Eocene|Overlies the Wangerrip Group. Unconformably overlain by the Heytesbury Group. Geological Province: Otway Basin.||||||
14185|Nirranda Group|24344|5|Briefly described|p69, 79|Oligocene|Eocene|||||||
14185|Nirranda Group|24551|5|Briefly described|p246|Oligocene|Eocene|Consists of: Mepunga Formation, Demons Bluff Formation, Narrawaturk Formation.||||||24-JUL-08
14185|Nirranda Group|24562|5|Briefly described|p7, 8, 35 Fig. 2|Oligocene|Eocene|Geological Province: Otway Basin.||||||
14185|Nirranda Group|29591|6|Mentioned|p91|||||||||
14185|Nirranda Group|29823|5|Briefly described|p14|||||||||
14185|Nirranda Group|29856|6|Mentioned|p41|||||||||
14185|Nirranda Group|30499|6|Mentioned|p92|||Stratigraphy||||||
14185|Nirranda Group|30578|4|Described|p9|||||||||
14185|Nirranda Group|30580|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
14185|Nirranda Group|30932|6|Mentioned|Map legend|Tertiary|Tertiary|Partly equivalent to Heytesbury Gp. & Glenelg Gp.||||||
14185|Nirranda Group|31036|1|Redefined|p210|middle Tertiary|middle Tertiary|Contains Narrawaturk Marl and Mepunga Formation.||||||31-JAN-07
14185|Nirranda Group|31372|6|Mentioned|p11|||||||||
14185|Nirranda Group|31424|6|Mentioned|Table 2|||Lithostratigraphy||||||
14185|Nirranda Group|31534|6|Mentioned|p369|||See also Table 19-3||||||
14185|Nirranda Group|31583|6|Mentioned|p18|||Section||||||
14185|Nirranda Group|31624|6|Mentioned|p101|||See also P111||||||
14185|Nirranda Group|31625|6|Mentioned|Fig. 5.2|||Eocene - Oligocene||||||
14185|Nirranda Group|32162|6|Mentioned|p58|||Fig.5||||||
14185|Nirranda Group|32852|6|Mentioned|p10|||||||||
14185|Nirranda Group|33940|6|Mentioned|p414|||||||||
14185|Nirranda Group|34063|6|Mentioned|p2|||Upper Eocene. Table||||||14-JAN-09
14185|Nirranda Group|35066|6|Mentioned|p208|||||||||
14185|Nirranda Group|35285|6|Mentioned|p414|||||||||
14185|Nirranda Group|36913|6|Mentioned|p81|||||||||
14185|Nirranda Group|38625|6|Mentioned|p272|||||||||
14185|Nirranda Group|38717|5|Briefly described|p20|||||||||
14185|Nirranda Group|39315|6|Mentioned|Fig.7|||||||||
14185|Nirranda Group|39446|6|Mentioned|p35|||||||||
14185|Nirranda Group|41016|5|Briefly described|Mention|||||||||
14185|Nirranda Group|41185|5|Briefly described|p175|||||||||
14185|Nirranda Group|41269|5|Briefly described|p246|||||||||
14185|Nirranda Group|41487|5|Briefly described|p625|||||||||
14185|Nirranda Group|41701|6|Mentioned|Map legend|middle Oligocene||||||||
14185|Nirranda Group|41704|6|Mentioned|p100|||||||||
14185|Nirranda Group|41714|6|Mentioned|p301|||||||||
14185|Nirranda Group|41726|6|Mentioned|p421|||||||||
14185|Nirranda Group|41769|4|Described|p25|||||||||
14185|Nirranda Group|41868|5|Briefly described|p535|||||||||
14185|Nirranda Group|42075|5|Briefly described|Fig.13 P252|||||||||
14185|Nirranda Group|42152|6|Mentioned|Fig.2 P4|||||||||
14185|Nirranda Group|42524|5|Briefly described|Fig.3 P27|||||||||
14185|Nirranda Group|42863|5|Briefly described|Fig.14|||Variation on Victorian unit.||||||
14185|Nirranda Group|43171|6|Mentioned|2-8|Oligocene|Middle Eocene|||||||
14185|Nirranda Group|43195|5|Briefly described|Map Legend||Eocene|See also commentary on back of map.||||||
14185|Nirranda Group|43208|5|Briefly described|map legend|Early Oligocene|Middle Eocene|||||||
14185|Nirranda Group|43219|5|Briefly described|Fig.3,p6.|Oligocene|Eocene|||||||
14185|Nirranda Group|43590|4|Described|p20|||||||||
14185|Nirranda Group|43604|6|Mentioned|p145|||||||||
14185|Nirranda Group|43660|6|Mentioned|Fig.6,p15|Oligocene|Eocene|||||||
14185|Nirranda Group|43667|6|Mentioned|Fig.3,p12||Eocene|||||||
14185|Nirranda Group|43733|6|Mentioned|Fig.2.11,p65|Oligocene|Eocene|||||||
14185|Nirranda Group|43744|6|Mentioned|Fig.3,p3|||||||||
14185|Nirranda Group|43783|6|Mentioned|Fig14, p11|Early Oligocene|Late Eocene|||||||
14185|Nirranda Group|43784|6|Mentioned|Fig10, p12|Early Oligocene|Late Eocene|||||||
14185|Nirranda Group|43814|6|Mentioned|Fig.3,p115|||||||||
14185|Nirranda Group|43937|5|Briefly described|Map Legend|Middle Eocene|Paleocene|||||||
14185|Nirranda Group|44133|5|Briefly described|p155|Late Eocene|Middle Eocene|Geological Province: Gambier Basin.  Includes: Mepunga Formation, Narrawaturk Marl.||||||
14185|Nirranda Group|46802|6|Mentioned|Table 1|||||||||
14185|Nirranda Group|48911|6|Mentioned|p49|||U.Eocene and Oligocene. Chart 1||||||
14185|Nirranda Group|48977|6|Mentioned|Fig.5|||See also Table 3||||||
14185|Nirranda Group|49060|5|Briefly described|Fig.33|||||||||
14185|Nirranda Group|60451|5|Briefly described|p95 Fig. 61|||||||||
14185|Nirranda Group|60452|5|Briefly described|p15|Eocene|Eocene|Age: 45Ma. Geological Province: Otway Basin.||||||
14185|Nirranda Group|60538|5|Briefly described|p470, Fig. 10, 473 Fig. 12, 474 Fig. 13|Early Oligocene|Late Eocene|Marl, littoral deposits. Includes: Gambier Limestone. Geological Province: Otway Basin.||||||
14185|Nirranda Group|60563|5|Briefly described|p45|||Carbonates. Includes the Narrawaturk Formation and Castle Cove Limestone. Overlies the Wangerrip Group. Geological Province: Otway Basin.||||||
14185|Nirranda Group|60599|5|Briefly described|p15|Middle Miocene|Middle Eocene|Fine-grained marginal marine sediments. Age: ~45Ma. Geological Province:Otway  Basin.||||||
14185|Nirranda Group|61182|3|Fully described|p20, p24, p36|Early Oligocene|Middle Eocene|Comprises Mepunga Fm and Narrawaturk Marl. Overlies Wangerrip Gp; overlain by Heytesbury Group. Formerly Nirranda Sub-group of the Heytesbury Gp; also known as Hanson Plain Sand in Heytesbury Group by some authors. Age: 45-29Ma.||||||
14185|Nirranda Group|61185|5|Briefly described|p15|Middle Miocene|Middle Eocene|Fine-grained marginal marine sediments. Geological Province: Otway Basin.||||||07-FEB-11
14185|Nirranda Group|61547|6|Mentioned|p461. |Eocene|Eocene|Written as Nirr. Group in the diagram, but shown in full, and in context, in the text on the same page.||||Overlies Wangerrip Group. Is overlain by Heytesbury Group.||
14185|Nirranda Group|61607|6|Mentioned|p5 Fig. 2|Oligocene|Eocene|Geological Province: Otway Basin.||||||12-MAR-09
14185|Nirranda Group|61608|6|Mentioned|p41 Fig. 5|||Refers to equivalent unit.||||||
14185|Nirranda Group|61622|4|Described|p436, p437, p436 Fig. 2|Miocene|Eocene|Includes Narrawaturk Marl. Geological Province: Otway Basin. Thin marls and carbonates deposited in mid to inner shelf environment.||||||07-FEB-11
14185|Nirranda Group|61623|5|Briefly described|p447, p449 Fig. 4|Tertiary|Tertiary|Includes Narrawaturk Marl and Mepunga Formation. Geological Province: Otway Basin.||||||07-APR-09
14185|Nirranda Group|61624|6|Mentioned|p465|Tertiary|Tertiary|Geological Province: Otway Basin.||||||07-APR-09
14185|Nirranda Group|61626|5|Briefly described|p486, p487, p486 Fig. 2, p488, p493|Oligocene|Eocene|Includes; Narrawaturk Marl, Mepunga Formation and Demons Bluff Formation. Geological Province: Otway Basin.||||||
14185|Nirranda Group|61627|5|Briefly described|p500 Fig. 2|Eocene|Eocene|Includes Mepunga Sandstone and Narrawaturk Marl. Geological Province: Otway Basin.||||||07-FEB-11
14185|Nirranda Group|61628|5|Briefly described|p509 Fig. 3|Early Oligocene|Middle Eocene|Includes Demons Bluff and Mepunga Formations and Narrawaturk Marl. Geological Province: Otway Basin.||||||07-APR-09
14185|Nirranda Group|62370|6|Mentioned|p455|||Geological Province: Otway Basin.||||||
14185|Nirranda Group|62896|6|Mentioned|p88|Tertiary|Tertiary|||||||07-FEB-11
14185|Nirranda Group|63122|5|Briefly described|p17 Fig. 4.3, p21|Late Eocene|Middle Eocene|Includes Narrawaturk Marl. Geological Province: Otway Basin. Presented in figure as Nirr. Gp.||||||
14185|Nirranda Group|63124|4|Described|p49 Fig. 5.2, p87 Fig. 5.29, p90-91|Late Eocene|Middle Eocene|Includes Narrawaturk Marl and Mepunga Formation. Geological Province: Otway Basin. Defined by Bock and Glenie (1965) but was downgraded to subgroup rank in the Heytesbury Group by some authors (Abele et al 1976); this was not generally accepted.||||||23-MAY-13
14185|Nirranda Group|63173|5|Briefly described|p342 Fig. 9.2|Late Oligocene|Middle Eocene|Geological Province: Otway Basin, offshore. Transgressive, shallow marine sedimentation.||||||07-FEB-11
14185|Nirranda Group|63269|5|Briefly described|p604-605|Oligocene|Eocene|Otway Basin.|||Demons Bluff, Mepunga Formations; Narrawaturk Marl.|Unconformably overlies Wangerrip Group. Is overlain unconformably by Heytesbury Group.||
14185|Nirranda Group|63431|5|Briefly described|p677 Fig. 2|Eocene|Eocene|Includes Narrawaturk Marl and Mepunga Formation.  Overlies Wangerrip Group; overlain by Heytesbury Group. Geological Province: Penola Trough/Otway Basin.||||||07-FEB-11
14185|Nirranda Group|63740|6|Mentioned|p88|Tertiary|Tertiary|||||||07-FEB-11
14185|Nirranda Group|65316|6|Mentioned|p597|||Largely subsurface; part of the Otway Basin; thought to correlate with the Demons Bluff Group.||||||23-APR-12
14185|Nirranda Group|65715|5|Briefly described|p11 Tb.7|Paleogene|Paleogene|Includes Narrawaturk Marl.||||||
14185|Nirranda Group|66002|5|Briefly described|p10 Tb.7, p16, p26 Fig.7|Paleogene|Paleogene|Includes Narrawaturk Marl and Mepunga Formation. Defined by Glenie 1971. Some outcrops in Port Campbell Embayment area reassigned to Wiridjil Gravel.||||||
14185|Nirranda Group|66181|6|Mentioned|p312|Eocene||Gippsland Basin||||||
14185|Nirranda Group|66245|5|Briefly described|p6 Fig.5, p8. |Rupelian|Lutetian|Coastal and shallow marine, progradational sequence of carbonates. Helped in building out the present day shelf.|||Includes Mepunga, Demons Bluff and ?Eastern View Formations and Narrawaturk Marl.|||
14185|Nirranda Group|67061|6|Mentioned|p546 Fig.3.|Oligocene|Eocene||||Includes Mepunga Formation and Narrawaturk Marl.|||
14185|Nirranda Group|67366|6|Mentioned|p103 Fig.2. |Oligocene|Eocene||||Includes Mepunga Formation and Narrawaturk Marl.|Unconformably overlies Wangerrip Group. Is unconformably overlain by Heytesbury Group.||
14185|Nirranda Group|67367|5|Briefly described|p130, p131 Fig.2. |Early Oligocene|Middle Eocene|Siliciclastics. Stratigraphic equivalent to Latrobe Group, offshore Gippsland Basin.|||Includes Mepunga, Demons Bluff and Narrawaturk Formations.|||
14185|Nirranda Group|69297|6|Mentioned|p78, p79, p98, p112, p115|Priabonian|Bartonian|Otway and Sorell Basins. Coastal plain to open marine siliciclastic and carbonate sediments. Potential reservoir in the Sorell Basin.|||Includes the Mepunga Formation, Narrawaturk Marl and the Wangoom Sand.|Unconformably overlies the Wangerrip Group. Overlain by the Heytesbury Group.||
14185|Nirranda Group|69651|5|Briefly described|p6, p10, p12, p32, p38|Miocene|Eocene|Otway Basin. Mixed carbonate/siliciclastic rocks. Modelling diagrams.|||Eastern View, Mepunga, Demons Bluff Formations; Narrawaturk Marl.|Unconformably overlies Wangerrip Group. Is overlain unconformably by Heytesbury Group.||
14185|Nirranda Group|69879|5|Briefly described|p418, p424|Oligocene|Eocene|Strahan Sub-basin. Shown as Nirranda Group equivalent. Offshore exploration well Cape Sorell 1.||||Overlies Wangerrip Group. Underlies Heytesbury Group.|Alternating beds of silty claystone/clayey siltstone (with organic content and terrestrial input) with clastics, and quartzitic sandstone. Fine sandstone and calcareous mudstone deposited in a shelfal marine environment.|
14185|Nirranda Group|70077|5|Briefly described|Nelson: Fig.2. Regional: Fig.4; p5|Oligocene|Eocene|Otway Basin: Gambier Embayment and Voluta Trough. Prograding nearshore to offshore marine clastics grading upwards into increasingly open marine carbonates.|||Narrawaturk Marl, Mepunga Formation, Wangoom Sand.|Overlies Wangerrip Group. Is overlain by Heytesbury Group.||
14185|Nirranda Group|70078|5|Briefly described|Northern: Fig.2; p2. Regional: Fig.4; p5|Eocene|Eocene|Otway Basin. Sandstones equivalent to this unit in the Sorell Basin are potential hydrocarbon sources; sealed by Heytesbury Group marls and fine-grained carbonates.|||Mepunga Formation, Narrawaturk Marl.|Overlies Wangerrip Group. Is overlain by Heytesbury Group.||
14185|Nirranda Group|70379|6|Mentioned|p724-727|||Otway Basin.||||Overlies Wangerrip Group. Is overlain by Heytesbury Group.||
14185|Nirranda Group|71437|4|Described|Fig. 1 opp 154, p155, p159-160|Oligocene|Eocene|Marine sediments include foraminifera and macrofossils.|||Includes Mepunga Group, Narrawaturk Marl.|Disconformably overlies Wangerrip Group. Overlain by Heytesbury Group.|Marl-sandy limestone suite.|
14185|Nirranda Group|71593|5|Briefly described|p51|Miocene|Oligocene|||||||
14185|Nirranda Group|73356|6|Mentioned|p3, p15-16|Oligocene|Eocene|Prograding marine clastics and carbonates.||||Unconformably overlain by Heytesbury Group.||
14185|Nirranda Group|73357|6|Mentioned|p44, p46, p48|Rupelian|Bartonian|Otway Basin.|||Includes Mepunga Formation, Narrawaturk Marl.|Overlies Wangerrip Group, underlies Heytesbury Group.||
14185|Nirranda Group|73383|4|Described|p3, p7 Tb.3.1, p10, p21, p27|Oligocene|Eocene|Otway Basin. Mid to late Eocene. Clastic units of Nirranda Group are equivalent to chemostratigraphic Sequence S5 which has generally lower Ti/Th values than other sequences in the Otway Basin. Carbonate units are equivalent to chemostratigraphic Sequence S6, primarily defined by high Ca values.|||Narrawaturk Marl, Demons Bluff Formation, Mepunga Formation|Overlies Wangerrip Group, underlies Heytesbury Group|Clastic and carbonate units including sandstones, mudstones, marls and calcareous mudstones.|
14185|Nirranda Group|73385|5|Briefly described|p3-5|Oligocene|Eocene|Otway Basin. Overlies intra-Lutein unconformity from localised inversion, underlies intra-Oligocene unconformity.|||Demons Bluff Formation, Mepunga Formation, Narrawaturk Marl|Unconformably overlies Wangerrip Group, unconformably underlies Heytesbury Group.|Prograding marine clastics and carbonates.|
14185|Nirranda Group|73386|4|Described|p1-2, p4-7, p13-14, iii, Attachment A1|Rupelian|Bartonian|Otway Basin, absent along northern margin. Thins to the northeast, onlapping the top of the Wangerrip Group or the top of the Eumeralla Formation. Represents change from siliciclastic to carbonate-dominated deposition with flooding of marine margin, chemostratigraphic division into sequences S5 and S6 of Forbes et al. (2020). Separated from underlying Wangerrip Group by an intra-Lutetian unconformity. Nothofagidites asperus to Lower Proteacidites tuberculatus spore-pollen zones.|||Narrawaturk Marl, Mepunga Formation|Unconformably overlies Wangerrip Group, unconformably underlies Heytesbury Group|Marine clastics and carbonates.|
14185|Nirranda Group|73486|5|Briefly described|p511 Fig.2, p516|Rupelian|Lutetian|Otway Basin.|||Eastern View Formation, Demons Bluff Formation, Mepunga Formation, Narrawaturk Marl|Underlies Heytesbury Group||
14185|Nirranda Group|73594|5|Briefly described|p4-5|Oligocene|Eocene|Otway Basin. Maximum thickness of ~200m in onshore areas, reaches 800m at the present-day shelf break.|||Demons Bluff Formation, Mepunga Formation, Narrawaturk Marl|Overlies Wangerrip Group, underlies Heytesbury Group||
14214|Nonowie Member|30804|6|Mentioned|p14|||On Table 1||||||
14214|Nonowie Member|31532|4|Described|Table 1|||||||||
14255|Normanville Group|22573|5|Briefly described|p 47||Cambrian|U-Pb zircon age 526Ma||||||
14255|Normanville Group|22581|5|Briefly described|Fig.2,p37||Cambrian|Kanmantoo Basin||||||
14255|Normanville Group|22603|6|Mentioned|p99||Early Cambrian|540 Ma (?)||||||
14255|Normanville Group|22634|5|Briefly described|p506|Cambrian|Neoproterozoic|||||||
14255|Normanville Group|22643|5|Briefly described|p186, fig3p187|Early Cambrian|Early Cambrian|||||||
14255|Normanville Group|22671|6|Mentioned|p846,848||Early Cambrian|Max Age: 526 (+/-) 4 Ma. Top of the group generally equated with Truro Volcanics.||||||18-JAN-06
14255|Normanville Group|22726|6|Mentioned|p233||Early Cambrian|||||||
14255|Normanville Group|22755|4|Described|p547, p548, p555||Early Cambrian|Of Stansbury Basin.||||||03-FEB-09
14255|Normanville Group|22766|4|Described|Fig.2 p561, p562||Tommotian|||||||
14255|Normanville Group|22772|5|Briefly described|Table 13.1|Early Cambrian|Early Cambrian|||||||
14255|Normanville Group|22830|6|Mentioned|P25||Cambrian|||||||
14255|Normanville Group|22857|5|Briefly described|Tb. 13.1 (insert p70-71), p88 Fig. 14.7A|Early Cambrian|Early Cambrian|Of the Moralana Supergroup. Age: <545Ma. Geological Province: Kanmantoo Trough; in the Stansbury Basin also. See also p93-94.||||||03-MAY-13
14255|Normanville Group|22858|6|Mentioned|p93,Fig14.7ap88-9|||||||||
14255|Normanville Group|23023|6|Mentioned|p1797|||||||||
14255|Normanville Group|23309|5|Briefly described|p26-27, 40, 46, 195||Cambrian|||||||
14255|Normanville Group|23317|5|Briefly described|377|Early Cambrian|Early Cambrian|||||||
14255|Normanville Group|23539|5|Briefly described|p 467|||||||||
14255|Normanville Group|23854|6|Mentioned|p863|||||||||
14255|Normanville Group|23869|5|Briefly described|p15 Fig. 3|Cambrian|Cambrian|||||||
14255|Normanville Group|23932|5|Briefly described|p667|Early Cambrian|Early Cambrian|Geological province: Adelaide Fold Belt.||||||
14255|Normanville Group|23981|5|Briefly described|p13, p20|Early Cambrian|Early Cambrian|Thickness: ~1000m. Geological Province: Stansbury (Fleurieu Peninsula) Basin. Comprises basal sandstones, shelf and ramp carbonates and includes relatively deep water phosphatic Heatherdale Shale.||||||04-FEB-08
14255|Normanville Group|24465|5|Briefly described|p343|Early Cambrian|Early Cambrian|Overlain by Kanmantoo Group. Geological Province: Stansbury Basin.||||||31-JAN-08
14255|Normanville Group|24551|5|Briefly described|p74|Cambrian|Cambrian|Of the Moralana Supergroup in SA.||||||
14255|Normanville Group|30381|6|Mentioned|p222|||||||||
14255|Normanville Group|32457|6|Mentioned|p88|||||||||
14255|Normanville Group|33471|5|Briefly described|p555|||||||||
14255|Normanville Group|34615|6|Mentioned|p7|||Shown on Figure.||||||
14255|Normanville Group|35092|6|Mentioned|p108|||||||||
14255|Normanville Group|35255|6|Mentioned|Fig.8|||||||||
14255|Normanville Group|36731|5|Briefly described|p124|||||||||
14255|Normanville Group|37461|6|Mentioned|Table 5.I|||||||||
14255|Normanville Group|38004|6|Mentioned|Table 1|||||||||
14255|Normanville Group|38157|6|Mentioned|Table V|||||||||
14255|Normanville Group|38703|6|Mentioned|p131|||||||||
14255|Normanville Group|38704|6|Mentioned|p133|||||||||
14255|Normanville Group|38873|4|Described|Table 2|||||||||
14255|Normanville Group|39344|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
14255|Normanville Group|39352|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
14255|Normanville Group|39489|6|Mentioned|Fig.1|||||||||
14255|Normanville Group|39806|6|Mentioned|p207|||||||||
14255|Normanville Group|39842|6|Mentioned|p5|||||||||
14255|Normanville Group|40228|5|Briefly described|Fig.1|||||||||
14255|Normanville Group|40442|4|Described|p13|||||||||
14255|Normanville Group|40454|6|Mentioned|p43|||||||||
14255|Normanville Group|40455|5|Briefly described|p67|||||||||
14255|Normanville Group|40456|6|Mentioned|Fig.2|||||||||
14255|Normanville Group|40503|4|Described|p107|||||||||
14255|Normanville Group|40763|5|Briefly described|p206|||||||||
14255|Normanville Group|40852|6|Mentioned|p32|||||||||
14255|Normanville Group|41103|6|Mentioned|p261|||||||||
14255|Normanville Group|41401|5|Briefly described|p32|||||||||
14255|Normanville Group|41526|6|Mentioned|p3|||See also P11||||||
14255|Normanville Group|41853|6|Mentioned|p195|||||||||
14255|Normanville Group|41947|6|Mentioned|p16|||||||||
14255|Normanville Group|42222|4|Described|p20|||||||||
14255|Normanville Group|42225|6|Mentioned|Fig.4 P224|||||||||
14255|Normanville Group|42232|6|Mentioned|p283|||||||||
14255|Normanville Group|42243|5|Briefly described|p207|||||||||
14255|Normanville Group|42266|6|Mentioned|p290|||||||||
14255|Normanville Group|42268|5|Briefly described|p328|||||||||
14255|Normanville Group|42269|6|Mentioned|Fig.1 P335|||||||||
14255|Normanville Group|42270|5|Briefly described|p353|||||||||
14255|Normanville Group|42271|5|Briefly described|p386|||||||||
14255|Normanville Group|42272|6|Mentioned|Fig.2 P400|||||||||
14255|Normanville Group|42275|5|Briefly described|p468|||||||||
14255|Normanville Group|42357|5|Briefly described|p10|||||||||
14255|Normanville Group|42488|5|Briefly described|p185, Fig.2 p187|||||||||
14255|Normanville Group|42505|5|Briefly described|Map legend|Cambrian||||||||
14255|Normanville Group|42506|5|Briefly described|Map legend|Early Cambrian||||||||
14255|Normanville Group|42600|6|Mentioned|p10|||||||||
14255|Normanville Group|42788|6|Mentioned|p148|||||||||
14255|Normanville Group|42982|6|Mentioned|Table 1,p333|||||||||
14255|Normanville Group|43052|5|Briefly described|Fig.2.14|||||||||
14255|Normanville Group|43053|5|Briefly described|Map Legend|Cambrian|Cambrian|Marine shelf to basinal carbonate, minor basal sandstone.||||||25-MAY-05
14255|Normanville Group|43190|5|Briefly described|Fig.1,p28.|||||||||
14255|Normanville Group|43192|6|Mentioned|p58||Cambrian|||||||
14255|Normanville Group|43258|5|Briefly described|Map Legend||Cambrian|||||||
14255|Normanville Group|43298|5|Briefly described|Map Legend||Cambrian|||||||
14255|Normanville Group|43595|6|Mentioned|p545||Cambrian|||||||
14255|Normanville Group|43703|6|Mentioned|p75|||||||||
14255|Normanville Group|43759|6|Mentioned|p446|||||||||
14255|Normanville Group|44133|5|Briefly described|p6, 18, 50|Cambrian|Cambrian|Metasediments and volcanics. Includes: Angaston Marble.||||||
14255|Normanville Group|50154|5|Briefly described|p22, p65|Early Cambrian|Early Cambrian|Of the Moralana Supergroup. Overlain by the Kanmantoo Group. Geological Province: Stansbury Basin.||||||16-SEP-04
14255|Normanville Group|60567|5|Briefly described|p39, 41|||Includes the Heatherdale Shale.||||||
14255|Normanville Group|60712|5|Briefly described|p27, p28 Fig. 1|Early Cambrian|Early Cambrian|Metamorphosed clastics and carbonates. Overlain by Kanmantoo Group. Geological Province: Kanmantoo Trough (Adelaide Geosyncline).||||||31-MAY-05
14255|Normanville Group|60953|5|Briefly described|Map Legend|Cambrian|Cambrian|Marine shelf to basinal carbonate, minor basal sandstone. Includes acid to basic volcanics near the Murray River.||||||
14255|Normanville Group|61046|5|Briefly described|p8 Fig. 2|Early Cambrian|Early Cambrian|Black shale, limestone. Includes Truro Volcanics.||||||
14255|Normanville Group|61108|5|Briefly described|map legend|Cambrian|Cambrian|Marine shelf to basinal carbonate; minor basal sandstone.||||||
14255|Normanville Group|61307|5|Briefly described|p3-4 Figs. 1 and 2|||Max. thickness: ~1km. Geological Province: Adelaide Fold Belt. See also p23.||||||15-JAN-08
14255|Normanville Group|62664|5|Briefly described|p138 Fig.2.|Cambrian|Early Cambrian|||||Unconformably overlies Wilpena Group of Heysen Supergroup.|Siltstone, carbonates, sandstone.|
14255|Normanville Group|63020|5|Briefly described|p973|Early Cambrian|Early Cambrian|||||||
14255|Normanville Group|63124|6|Mentioned|p49|||Geological Province: Otway Basin.||||||
14255|Normanville Group|63848|6|Mentioned|p533 Fig.2,  p534 Fig.4.||||||Includes Mount Terrible, Wangkonda and Sellick Hill Formations; Fork Tree Limestone; Truro Volcanics and Heatherdale Shale.|||
14255|Normanville Group|64281|5|Briefly described|p29|Cambrian|Cambrian|On Yorke Peninsula, Fleurieu Peninsula. Correlate with Kangaroo Island Group.||||||23-DEC-09
14255|Normanville Group|64647|5|Briefly described|p38 Fig. 1, p46|||Overlies Burra Group. Marine sediments.||||||
14255|Normanville Group|65375|5|Briefly described|p33.|Cambrian|Cambrian|Correlative of Hawker Group above that unit's Uratanna Formation.|||Includes Mount Terrible, Wangkonda and Sellick Hill Formations; Fork Tree Limestone and Heatherdale Shale.|Is overlain by Kanmantoo Group.||
14255|Normanville Group|65376|6|Mentioned|p92 Fig. 2.82. |Cambrian|Cambrian|||||||
14255|Normanville Group|65379|5|Briefly described|p643|||Of Moralana Supergroup. Includes Heatherdale Shale and Angaston Marble. Asbestos occurrence hosted in dolomite and/or limestones in this group.||||||07-MAR-12
14255|Normanville Group|65664|5|Briefly described|p1096, p1103, p1106 Fig.5|Early Cambrian|Early Cambrian||||Includes Heatherdale Shale and Sellicks Hill Formation.|Unconformably overlain by Kanmantoo Group. Unconformably overlies Wilpena Group.||09-MAY-12
14255|Normanville Group|65686|6|Mentioned|p408|||Of the Fleurieu Peninsula. Includes a few poorly preserved trilobites.||||||07-MAY-12
14255|Normanville Group|65892|5|Briefly described|p9 Fig.4, p13, p16, p19.|Early Cambrian|Early Cambrian|Fleurieu Peninsula.|||Includes Mount Terrible, Wangkonda, Sellick Hill Formations; Fork Tree Limestone; Heatherdale Shale; Truro Volcanics.|Is overlain by Kanmantoo Group.||
14255|Normanville Group|67103|6|Mentioned|p612|||||||||
14255|Normanville Group|67536|4|Described|Map Legend|Stage 3|Stage 2|Kanmantoo Province; basement to Murray Basin.|522 +/- 2 Ma|||Intercalated wuth Truro Volcanics.|Marine shelf to basinal carbonate, minor basal sandstone and tuff.|
14255|Normanville Group|68735|5|Briefly described|p233 Fig.2, p235 Fig.3|Early Cambrian|Early Cambrian|Stansbury Basin.|||Includes Mount Terrible Formation, Wangkonda Formation, Sellick Hill Formation, Fork Tree Limestone, Heatherdale Shale and Truro Volcanics.|Is overlain by Kanmantoo Group.||10-APR-17
14255|Normanville Group|68822|5|Briefly described|p324|Cambrian|Cambrian|Shallow water depositional environment.|||Includes the Truro Volcanics.|Overlain by the Kanmantoo Formation.||
14255|Normanville Group|68993|5|Briefly described|p544 Fig.1|Early Cambrian|Early Cambrian||||Includes Heatherdale Shale, Truro Volcanics, Fork Tree Limestone; Sellick Hill, Wangkonda and Mount Terrible Formations.|||28-JUL-15
14255|Normanville Group|69255|6|Mentioned|p771|Cambrian|Cambrian||Between 522-515 Ma.|||||
14255|Normanville Group|70125|6|Mentioned|p400 Tb.5||||522 Ma (tuff).|||||
14255|Normanville Group|70493|6|Mentioned|p56|Early Cambrian|Early Cambrian|Delamerian Orogen, SA.||||Is overlain by Kanmantoo Group.||
14255|Normanville Group|71139|6|Mentioned|p152-153, 161|||Adelaide Geosyncline.|c.526 Ma.||Heatherdale Shale.|Is overlain by Kanmantoo Group.||
14255|Normanville Group|71322|5|Briefly described|p52 Fig.1, p73-74|Cambrian|Cambrian||||Marne River Volcanics, Truro Volcanics.|Intrercalated with Truro Volcanics.|Limestone, sandstone, shale, volcanics.|
14255|Normanville Group|71593|5|Briefly described|p19-p21, p170|Early Cambrian|Early Cambrian|||Moralana Supergroup||Unconformably overlies the Heysen Supergroup. Disconformably overlain by the Kanmantoo Group.|Shallow marine sediments including fossiliferous shale and sandstone, limestone, marble, calcareous dolomite and fossiliferous shale.|
14255|Normanville Group|72450|5|Briefly described|Brochure, Brochure map|Early Cambrian|Early Cambrian|Contains some of the oldest shelly fossils (cup-shaped double walled archaeocyaths). Deformed by the Delamerian Orogeny.|||Includes the Heatherdale Shale, Fork Tree Limestone, Sellick Hill Formation, Wangkonda Formation and Mount Terrible Formation.|Overlies the ABC Range Quartzite.||
14255|Normanville Group|73059|5|Briefly described|p1059, 1061|Early Cambrian|Early Cambrian|Delamerian Fold Belt, South Australia. Formed in a synorogenic basinal setting, not in an extensional basin setting.|||Heatherdale Shale, Mount Terrible Formation.|Is overlain by Kanmantoo Group.|Shallow marine succession.|
14255|Normanville Group|73129|6|Mentioned|p45|||||||||
14255|Normanville Group|73188|5|Briefly described|p315-316, p343, p349-351, p353|Early Cambrian|Early Cambrian|Mount Lofty Ranges. Shelf sediments. Records marine transgression and overall upward deepening.|||Heatherdale Shale, Fork Tree Limestone, Sellick Hill Formation, Wangkonda Formation, Mount Terrible Formation|Disconformably underlain by ABC Range Quartzite and Bunyeroo Formation. Disconformably overlain by Kanmantoo Group.|Carbonate dominated with sands and silts.|
14255|Normanville Group|73236|6|Mentioned|p47|Cambrian|Cambrian|Fleurieu Peninsula; eroded from the Hallett Cove area.|c. 530-510 Ma||||Carbonate-dominated.|
14255|Normanville Group|73264|6|Mentioned|p1387 Fig.10, p1388|||Grenvillian zircon population (1000-1200 Ma), small Panafrican peak at 645 Ma.|||Heatherdale Shale, Mount Terrible Formation|||
14255|Normanville Group|73430|5|Briefly described|p491-p493, p497|Early Cambrian|Early Cambrian|Delamerian Orogen. Records rapidly increasing water depth towards the Heatherdale Shale. Deformed in the middle to late Cambrian.|||Truro Volcanics|Underlies Kanmantoo Group|Carbonates. Includes alkali basalt lavas.|
14255|Normanville Group|74367|5|Briefly described|p6, p19|Cambrian|Cambrian|||Moralana Supergroup|Heatherdale Shale||Limestone, sandstone, shale and volcanics.|
14306|Norwest Bend Formation|9124|5|Briefly described|Map Legend|Pliocene|Pliocene|Marine sandy limestone of the Murray River area.||||||
14306|Norwest Bend Formation|22773|5|Briefly described|Fig24.8p352+24.9p353|Late Pliocene|Late Pliocene|||||||
14306|Norwest Bend Formation|22799|5|Briefly described|p23 Fig.7|Pliocene|Pliocene|||||||
14306|Norwest Bend Formation|22857|5|Briefly described|p352-3 Figs.24.8 and 24.9|Late Pliocene|Late Pliocene|Geological Province: Murray Basin.||||||
14306|Norwest Bend Formation|22887|5|Briefly described|Fig.6 p13|Late Pliocene|Late Pliocene|||||||
14306|Norwest Bend Formation|22893|5|Briefly described|p34 fig9|Pliocene|Pliocene|Fossil rich||||||
14306|Norwest Bend Formation|23226|6|Mentioned|p901|||May overlap Pata Formation depending upon geographic location.  Of Murray Basin.||||||
14306|Norwest Bend Formation|23768|5|Briefly described|p30 Fig.6, p27, p57|Late Pliocene|Late Pliocene|Geological Province: Murray Basin.  Overlies Bookpurnong Formation.||||||
14306|Norwest Bend Formation|23818|5|Briefly described|p174 Fig.84, p186|Pliocene|Pliocene|Geological Province: Murray Basin. Underlying unit: Loxton Sands.||||||
14306|Norwest Bend Formation|23884|5|Briefly described|p155 Fig.13.2|Pliocene|Pliocene|Geological Province: Murray Basin.||||||
14306|Norwest Bend Formation|29591|6|Mentioned|p90|||||||||
14306|Norwest Bend Formation|29697|5|Briefly described|Table 1|||||||||
14306|Norwest Bend Formation|30750|6|Mentioned|p1|||||||||
14306|Norwest Bend Formation|30751|6|Mentioned|Map legend|late Pliocene|late Pliocene|||||||
14306|Norwest Bend Formation|30753|4|Described|p15|||Upper Pliocene age||||||
14306|Norwest Bend Formation|30754|5|Briefly described|p14|||Stratigraphic tables. See also p22. Section p42.||||||07-SEP-18
14306|Norwest Bend Formation|30757|6|Mentioned|p4|||||||||
14306|Norwest Bend Formation|30807|6|Mentioned|p101|||Suggested map symbol||||||
14306|Norwest Bend Formation|31625|6|Mentioned|Fig. 5.2|||Upper Pliocene.||||||29-JUL-08
14306|Norwest Bend Formation|31848|4|Described|p12|||U.Pliocene||||||
14306|Norwest Bend Formation|31923|6|Mentioned|p17|||||||||
14306|Norwest Bend Formation|32432|4|Described|Table 1|||||||||
14306|Norwest Bend Formation|32653|6|Mentioned|p295|||||||||
14306|Norwest Bend Formation|32862|5|Briefly described|Table 3|||||||||
14306|Norwest Bend Formation|32864|6|Mentioned|Table 1|||Fig. 5 only||||||
14306|Norwest Bend Formation|34029|5|Briefly described|Table 1|||Aquifer. U.Pliocene||||||
14306|Norwest Bend Formation|34114|4|Described|p50|||Upper Pliocene||||||
14306|Norwest Bend Formation|34180|5|Briefly described|p212|||Late Pliocene. Equivalent Parilla Sand.||||||
14306|Norwest Bend Formation|34296|5|Briefly described|p95|||||||||
14306|Norwest Bend Formation|34308|5|Briefly described|p186|||Yatalan.||||||07-SEP-18
14306|Norwest Bend Formation|34461|5|Briefly described|p49|||||||||
14306|Norwest Bend Formation|34536|6|Mentioned|Map legend|Pliocene|Pliocene|||||||
14306|Norwest Bend Formation|34758|6|Mentioned|Fig.2|||See also mention Table 1||||||
14306|Norwest Bend Formation|35097|6|Mentioned|Fig.4|||||||||
14306|Norwest Bend Formation|35200|6|Mentioned|Map legend|Pliocene|Pliocene|||||||
14306|Norwest Bend Formation|35232|5|Briefly described|Table.3|||||||||
14306|Norwest Bend Formation|35541|6|Mentioned|Fig.2|||Geological section of Tertiary and Quaternary sediments||||||
14306|Norwest Bend Formation|37619|6|Mentioned|p2|||||||||
14306|Norwest Bend Formation|38070|6|Mentioned|Fig.12|||Murray Basin||||||
14306|Norwest Bend Formation|39329|6|Mentioned|Fig.1|||||||||
14306|Norwest Bend Formation|39352|6|Mentioned|Map legend|Pliocene|Pliocene|||||||
14306|Norwest Bend Formation|40003|5|Briefly described|Table 8|||||||||
14306|Norwest Bend Formation|40215|6|Mentioned|p56|||||||||
14306|Norwest Bend Formation|40820|6|Mentioned|Fig.4|||||||||
14306|Norwest Bend Formation|41075|6|Mentioned|p25|||||||||
14306|Norwest Bend Formation|41511|5|Briefly described|p18|||||||||
14306|Norwest Bend Formation|41537|6|Mentioned|fig.2|||||||||
14306|Norwest Bend Formation|42115|6|Mentioned|p7|||||||||
14306|Norwest Bend Formation|42125|5|Briefly described|p139|||See also Fig.5||||||
14306|Norwest Bend Formation|42126|6|Mentioned|Fig.2 P148|||||||||
14306|Norwest Bend Formation|42130|6|Mentioned|Fig.3 P265|||||||||
14306|Norwest Bend Formation|42134|6|Mentioned|Fig.3 P335|||||||||
14306|Norwest Bend Formation|42137|5|Briefly described|Fig 2 P368|||||||||
14306|Norwest Bend Formation|42138|6|Mentioned|p392|||||||||
14306|Norwest Bend Formation|42443|4|Described|p4|||||||||
14306|Norwest Bend Formation|42717|5|Briefly described|map legend|Pliocene||||||||
14306|Norwest Bend Formation|42813|6|Mentioned|p25|||||||||
14306|Norwest Bend Formation|42881|4|Described|Fig.3, P84|||||||||
14306|Norwest Bend Formation|42966|2|Defined|p175|Late Pliocene||||||||
14306|Norwest Bend Formation|43073|4|Described|p13,Table 3|||||||||
14306|Norwest Bend Formation|43655|5|Briefly described|p40-846|||||||||
14306|Norwest Bend Formation|43791|6|Mentioned|p372, Fig1|||||||||
14306|Norwest Bend Formation|43804|6|Mentioned|Fig.2,p49|||||||||
14306|Norwest Bend Formation|44133|5|Briefly described|p161|Late Pliocene|Late Pliocene|Geological Province: Murray Basin.||||||
14306|Norwest Bend Formation|49038|4|Described|Table 2|||||||||
14306|Norwest Bend Formation|49040|6|Mentioned|p12|||||||||
14306|Norwest Bend Formation|60540|5|Briefly described|p998-1024|Late Pliocene|Early Pliocene|~15 m thick. In the western Murray Basin. Not a single stratigraphic unit. Transgresive systems tract. Divided into two unconformity-bounded informal members: lower quartzose sand member; upper oyster-rich member. Both (informal) members include fossil fauna. Facies described in great detail. Ages from magnetostratigraphy in Moorna Formation, and biostratigraphy in this and Bookpurnong Fm. See also Northwest Bend Formation (as it is written in some of the diagrams; abbreviated to NW Bend Formation).|~4.6-3.8 and ~3.4-2.4 Ma|||Lower member grades laterally into Loxton Sand, upper member grades laterally into Parilla Sand.|Well-preserved succession of terrestrial and shallow-marine deposits. Includes mollusc-rich sandy limestones.|06-FEB-18
14306|Norwest Bend Formation|60953|5|Briefly described|Map Legend|Pliocene|Pliocene|Esturine sandy limestone, calcareous sandstone and oyster beds.||||||
14306|Norwest Bend Formation|61108|5|Briefly described|map legend|Pliocene|Pliocene|Estuarine sandy limestone, calcareous sandstone and oyster beds.||||||
14306|Norwest Bend Formation|61155|5|Briefly described|p5 |Pliocene|Pliocene|Estuarine oyster beds of the ancestral Murray River||||||
14306|Norwest Bend Formation|61207|5|Briefly described|p280 Fig. 2|Late Pliocene|Late Pliocene|Geological Province: Murray Basin.||||||
14306|Norwest Bend Formation|64237|5|Briefly described|p18 Fig. 2, p19 Fig. 2b, p20|Late Pliocene|Late Miocene|Included in the original stratigraphic scheme for the Murray Group.  Correlated with Parilla Sand. Overlies Loxton Sand. There is a proposal to extend the unit downwards so that it also correlates with the Early Pliocene Loxton Sand.||||||25-FEB-13
14306|Norwest Bend Formation|64961|5|Briefly described|p260|Late Pliocene||Overlain by Blanchetown Clay in western part of basin. Geological province: Murray Basin. Exhibits well-developed karst topography.||||||21-APR-09
14306|Norwest Bend Formation|65552|5|Briefly described|p5 Fig. 3|Late Pliocene|Late Pliocene|Limestone of the western Murray Basin. Overlies Loxton Sands, underlies (toward the east) Blanchetown Clay  and (toward the west) surface aeolian-fluvio-lacustrine deposits (e.g. Woorinen Formation, Coonambidgal Formation, Molineaux-Lowan Sands).||||||
14306|Norwest Bend Formation|66286|6|Mentioned|pp180-181.|||Includes two informal members. The lower quartzose one grades into the Loxton Sands, while the upper, oyster-rich one grades into the coeval Parilla Sand.||||||
14306|Norwest Bend Formation|66287|5|Briefly described|Fig 2,5, p28, 33,35,40,Fig 17|Early Pliocene|Late Miocene|Oyster-dominated estuarine facies overlies a sand and gravel dominated facies. Estuarine facies of both units may be considered equivalent.||||Overlies the Loxton-Parilla Sands.||20-APR-12
14306|Norwest Bend Formation|68548|5|Briefly described|p11, p13-21|Pliocene|Pliocene|Informally subdivided into lower and upper parts. Late Pliocene age. Upper member comprises a ~ 15m thick flat-lying unit deposited between ca. 3.4-2.3 Ma. Monospecific Ostrea angasi deposits form bioherms, biostromes and subaqueous dunes.||||Grades into the Loxton Sand to the east. Laterally equivalent to the Parilla Sand. Upper part laterally equivalent to the Moorna Formation.|Quartzose sands (lower); limestones of oyster-rich sediments (upper).|
14306|Norwest Bend Formation|70718|6|Mentioned|p129|||||||Overlies Loxton Sand.||
14306|Norwest Bend Formation|71248|14|Not recorded|p2||Pliocene|||||||
14306|Norwest Bend Formation|72445|6|Mentioned|App.7 p7 Fig.4.|Pliocene|Pliocene|Shown on the 'Lithostratigraphy of Cenozoic sediments in the Murray Basin' (from Brown & Stephenson 1991).||||Shown as overlying Loxton Sands and being equivalent to Parilla Sand and partially underlying Blanchetown Clay.|Shown as including limestone.|
14306|Norwest Bend Formation|73118|5|Briefly described|p17, 81|Pliocene|Pliocene|Exposed in cliffs of River Murray gorge. Estuarine deposits.|||||Partly cemented pale grey, brown, yellow coquinoid limestone with fossiliferous quartz sand matrix; characterised by oyster beds.|
14306|Norwest Bend Formation|73188|6|Mentioned|p320|Pliocene|Pliocene|Murray Basin.|||||Shallow marine calcareous sand, fluvial and coastal barrier sands.|
14306|Norwest Bend Formation|73228|5|Briefly described|p50, p55-57, p59, p62|Early Pliocene|Late Miocene|Murray Basin. Deposited in a narrow estuarine zone extending northwards from Tailem Bend along the western margin of the basin between Overland Corner and Nildottie, where the Loxton Sand ridges are absent. Typically 15-20 m thick; maximum thickness of 45 m.||||Underlain by Loxton Sand. Unconformably underlain by Murray Group.|Fossiliferous sandy limestone, calcareous sandstone and oyster beds.|
14306|Norwest Bend Formation|73229|6|Mentioned|p67|Pliocene|Late Miocene|Murray Basin. [An informal upper subdivision is mentioned once but not explicetly as a distinct unit].||||||31-OCT-22
14317|Nowillilla Sandy Loam|38290|5|Briefly described|p61|||||||||
14329|Nuccaleena Formation|7931|5|Briefly described|p98, p99 Fig. 2|Ediacaran|Ediacaran|Of Sandison Subgroup (Wilpena Group). A 'cap dolostone' unit overlying the Marinoan glacials of the upper Umberatana Group; overlain by Brachina Formation.||||||07-FEB-11
14329|Nuccaleena Formation|9862|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Of the Wilpena Group. Yellow-brown weathering laminated and flaggy or well-bedded, grey-brown dolomite.||||||
14329|Nuccaleena Formation|22646|6|Mentioned|Fig 4 on p 102|Neoproterozoic|Neoproterozoic|Adelaide Geosyncline (West).  Age - Ediacarian in text.||||||
14329|Nuccaleena Formation|22649|6|Mentioned|p 152|||Province - Adelaide Geosyncline.||||||
14329|Nuccaleena Formation|22677|6|Mentioned|p734|||||||||
14329|Nuccaleena Formation|22772|5|Briefly described|Table13.1|Neoproterozoic III|Neoproterozoic III|||||||
14329|Nuccaleena Formation|22857|5|Briefly described|Tb. 13.1 (insert p70-71)|Precambrian|Precambrian|Of the Wilpena Group. Age: 590Ma.||||||24-MAR-06
14329|Nuccaleena Formation|22901|6|Mentioned|78|||Geol province Adelaide Rift Complex||||||
14329|Nuccaleena Formation|22921|6|Mentioned|37|||Parent Wilpena Group||||||
14329|Nuccaleena Formation|23180|6|Mentioned|p36, Fig.1|||Age: Adelaidean||||||
14329|Nuccaleena Formation|23211|5|Briefly described|p43-45 Fig.2|||Of Sandison Subgroup.||||||13-FEB-08
14329|Nuccaleena Formation|23250|5|Briefly described|p1122, p1124  Fig.2||Neoproterozoic III|of Wilpena Group. Correlate of Gayland Sandstone.||||||
14329|Nuccaleena Formation|23287|6|Mentioned|p104, Fig.2-4|||Age: Lower Ediacarian. of Wilpena Group, Adelaide Geosyncline and Stuart Shelf.||||||
14329|Nuccaleena Formation|23394|5|Briefly described|Map legend|Proterozoic|Proterozoic|||||||
14329|Nuccaleena Formation|23411|6|Mentioned|Map Legend|||||||||
14329|Nuccaleena Formation|23557|5|Briefly described|p95 Fig.1|Neoproterozoic III|Neoproterozoic III|Geological Province: Adelaide Rift Complex.||||||
14329|Nuccaleena Formation|23719|5|Briefly described|p26|||Of Wilpena Group. Geological Province: Gawler Craton.||||||
14329|Nuccaleena Formation|23806|5|Briefly described|p1122 Fig. 1|Neoproterozoic|Neoproterozoic|||||||
14329|Nuccaleena Formation|23818|4|Described|p73 Fig.27, p74|Adelaidean|Adelaidean|Lowermost unit of the Wilpena Group. Max. thickness: ~230 ft. overlying unit: Seacliff Sandstone Member.||||||
14329|Nuccaleena Formation|23913|4|Described|p108, p110 Fig. 2|Adelaidean|Adelaidean|Geological Province: Adelaide Geosyncline.  Of the Wilpena Group.  Underlain by Elatina Formation and Whyalla Sandstone. Overlain by Tent Hill Formation and Brachina Formation.||||||21-APR-09
14329|Nuccaleena Formation|24175|5|Briefly described|p13|Neoproterozoic|Neoproterozoic|Of the Wilpena Group.  Overlain by Brachina  Formation; overlies Brachina Formation.  Max. thickness: 3m.||||||
14329|Nuccaleena Formation|24176|4|Described|p24 Tb. 1, p14|Adelaidean|Adelaidean|Of the Wilpena Group. Purple shale, minor dolomite. Overlain by Brachina Formation. Max. thickness: 140m. Geological Province: Mount Painter Province.||||||14-APR-08
14329|Nuccaleena Formation|24195|5|Briefly described|p45 Fig.3|||Of the Sandison Subgroup. Geological Province: Adelaide Geosyncline||||||
14329|Nuccaleena Formation|24321|5|Briefly described|Map legend|Late Adelaidean|Late Adelaidean|Parent: Wilpena Group.||||||13-FEB-08
14329|Nuccaleena Formation|24476|4|Described|p547 Fig. 4|Vendian|Vendian|Overlies the Elatina Formation and the Whyalla Sandstone. Overlain by the Brachina Formation and Tent Hill Formation. Geological Province: Adelaide fold belt and Stuart Shelf.||||||16-SEP-08
14329|Nuccaleena Formation|24546|5|Briefly described|p2 - 3 Fig.2|Neoproterozoic|Neoproterozoic|Of Wilpena Group. Geological Province: Adelaide Fold Belt.||||||16-JAN-08
14329|Nuccaleena Formation|24586|5|Briefly described|p51 Fig. 1, p52 Fig. 3|Adelaidean|Adelaidean|Of the Sandison Subgroup (Wilpena Group). Onlapped by Brachina Formation; discordantly overlain by Ulupa Siltstone. Geological Province: Adelaide Geosyncline.||||||
14329|Nuccaleena Formation|29656|6|Mentioned|Fig.9|||||||||
14329|Nuccaleena Formation|29780|4|Described|p100|||||||||
14329|Nuccaleena Formation|29834|6|Mentioned|p198|||||||||
14329|Nuccaleena Formation|29837|6|Mentioned|p75|||||||||
14329|Nuccaleena Formation|30176|6|Mentioned|Map legend|Adelaidean|Adelaidean|Marinoan||||||
14329|Nuccaleena Formation|30177|4|Described|p88|||||||||
14329|Nuccaleena Formation|30261|6|Mentioned|Table 1|||Marinoan||||||
14329|Nuccaleena Formation|30798|6|Mentioned|p116|||See also Fig .1||||||
14329|Nuccaleena Formation|30801|6|Mentioned|p5|||Marinoan. Table P5-6||||||
14329|Nuccaleena Formation|30802|5|Briefly described|p12|||Marinoan age||||||
14329|Nuccaleena Formation|30807|6|Mentioned|p102|||Suggested map symbol||||||
14329|Nuccaleena Formation|31923|6|Mentioned|p10|||||||||
14329|Nuccaleena Formation|32146|6|Mentioned|Fig.3|||||||||
14329|Nuccaleena Formation|32504|6|Mentioned|Fig.2|||||||||
14329|Nuccaleena Formation|32505|6|Mentioned|Table 3|||||||||
14329|Nuccaleena Formation|32506|6|Mentioned|Fig.1|||||||||
14329|Nuccaleena Formation|32511|6|Mentioned|Fig.1|||||||||
14329|Nuccaleena Formation|32720|6|Mentioned|Table 1|||Wilpena Gp.||||||
14329|Nuccaleena Formation|32722|6|Mentioned|Fig.3|||Adelaidean. Stromatolite||||||
14329|Nuccaleena Formation|32724|6|Mentioned|Fig.1|||Correlation. Marinoan||||||
14329|Nuccaleena Formation|33036|6|Mentioned|Fig.2|||||||||
14329|Nuccaleena Formation|33037|6|Mentioned|Fig.2|||||||||
14329|Nuccaleena Formation|33474|6|Mentioned|Fig.2|||||||||
14329|Nuccaleena Formation|34175|6|Mentioned|p36|||||||||
14329|Nuccaleena Formation|34267|6|Mentioned|Fig.|||The Oraparinna & Enorama diapiric structures||||||
14329|Nuccaleena Formation|34269|6|Mentioned|Table 1|||||||||
14329|Nuccaleena Formation|34291|6|Mentioned|p18|||Adelaidean. See also P19||||||
14329|Nuccaleena Formation|34535|5|Briefly described|p74|||See Fig.27||||||
14329|Nuccaleena Formation|34536|6|Mentioned|Map legend|Adelaidean|Adelaidean|Marinoan||||||
14329|Nuccaleena Formation|34563|6|Mentioned|p67|||Correlation||||||
14329|Nuccaleena Formation|34812|6|Mentioned|p137|||||||||
14329|Nuccaleena Formation|34835|6|Mentioned|Fig.2|||||||||
14329|Nuccaleena Formation|34836|6|Mentioned|Fig.2|||||||||
14329|Nuccaleena Formation|35075|6|Mentioned|Fig.2|||||||||
14329|Nuccaleena Formation|35143|6|Mentioned|Fig.2|||||||||
14329|Nuccaleena Formation|35158|6|Mentioned|p47|||||||||
14329|Nuccaleena Formation|35195|6|Mentioned|Table 3|||||||||
14329|Nuccaleena Formation|35255|6|Mentioned|Fig.6|||||||||
14329|Nuccaleena Formation|35317|4|Described|p395|||Sedimentary facies & palaeoenvironments discussed. Upper Precambrian.||||||
14329|Nuccaleena Formation|35582|6|Mentioned|Fig.2|||||||||
14329|Nuccaleena Formation|35586|4|Described|p30|||Follows definition of Dalgarno and Johnson.||||||20-FEB-08
14329|Nuccaleena Formation|35675|6|Mentioned|Fig.1|||Location plan & regional geology.||||||
14329|Nuccaleena Formation|36048|6|Mentioned|p377|||||||||
14329|Nuccaleena Formation|36245|6|Mentioned|Fig.1|||||||||
14329|Nuccaleena Formation|36898|6|Mentioned|p196|||||||||
14329|Nuccaleena Formation|37015|6|Mentioned|Fig.2|||||||||
14329|Nuccaleena Formation|37461|6|Mentioned|Table 5.I|||||||||
14329|Nuccaleena Formation|37627|6|Mentioned|p187|||||||||
14329|Nuccaleena Formation|37932|5|Briefly described|p546|||||||||
14329|Nuccaleena Formation|38022|6|Mentioned|Fig.4|||||||||
14329|Nuccaleena Formation|38110|6|Mentioned|p2|||||||||
14329|Nuccaleena Formation|38157|6|Mentioned|Table V|||See also P287.||||||
14329|Nuccaleena Formation|38945|6|Mentioned|p130|||||||||
14329|Nuccaleena Formation|39210|6|Mentioned|Table 4|||||||||
14329|Nuccaleena Formation|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Marinoan||||||
14329|Nuccaleena Formation|39352|6|Mentioned|Map legend|Adelaidean|Adelaidean|Marinoan||||||
14329|Nuccaleena Formation|40442|5|Briefly described|p10|||||||||
14329|Nuccaleena Formation|40456|6|Mentioned|p21|||||||||
14329|Nuccaleena Formation|40914|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
14329|Nuccaleena Formation|41005|6|Mentioned|p419|||||||||
14329|Nuccaleena Formation|41236|5|Briefly described|p63|||||||||
14329|Nuccaleena Formation|41401|6|Mentioned|p32|||||||||
14329|Nuccaleena Formation|41429|3|Fully described|p211|||||||||
14329|Nuccaleena Formation|41500|6|Mentioned|Fig.1|||||||||
14329|Nuccaleena Formation|41794|6|Mentioned|Fig.2|||||||||
14329|Nuccaleena Formation|41801|6|Mentioned|p218|||||||||
14329|Nuccaleena Formation|42028|6|Mentioned|p137|||||||||
14329|Nuccaleena Formation|42090|5|Briefly described|p25|||||||||
14329|Nuccaleena Formation|42098|5|Briefly described|p54|||||||||
14329|Nuccaleena Formation|42222|6|Mentioned|Table 1 P4|||||||||
14329|Nuccaleena Formation|42235|5|Briefly described|p140|||||||||
14329|Nuccaleena Formation|42238|6|Mentioned|Table 1 P74|||||||||
14329|Nuccaleena Formation|42239|5|Briefly described|p157|||||||||
14329|Nuccaleena Formation|42240|5|Briefly described|p166|||||||||
14329|Nuccaleena Formation|42241|6|Mentioned|p178|||||||||
14329|Nuccaleena Formation|42243|6|Mentioned|p211|||||||||
14329|Nuccaleena Formation|42465|5|Briefly described|Map Legend|||||||||
14329|Nuccaleena Formation|42469|4|Described|p23|||||||||
14329|Nuccaleena Formation|42542|5|Briefly described|Fig. 2a P11|||||||||
14329|Nuccaleena Formation|42600|4|Described|p6|||||||||
14329|Nuccaleena Formation|42720|5|Briefly described|map legend|Marinoan||||||||
14329|Nuccaleena Formation|42763|5|Briefly described|p20|||see also Fig.2 P21, Fig.3 P23||||||
14329|Nuccaleena Formation|42813|5|Briefly described|p21|||of Wilpena Group||||||
14329|Nuccaleena Formation|42882|5|Briefly described|Fig.7 P12|||||||||
14329|Nuccaleena Formation|43048|6|Mentioned|p14|||||||||
14329|Nuccaleena Formation|43052|5|Briefly described|p192,Table 6.1|||of Wilpena Group||||||
14329|Nuccaleena Formation|43622|6|Mentioned|p38|Neoproterozoic||||||||
14329|Nuccaleena Formation|43845|5|Briefly described|Fig3 p43, 46||Neoproterozoic|In Wilpena Group||||||12-JUL-16
14329|Nuccaleena Formation|44659|5|Briefly described|map legend|||Marinoan, lithology.||||||
14329|Nuccaleena Formation|44660|14|Not recorded|map legend|||Marinoan, lithology.||||||
14329|Nuccaleena Formation|44689|14|Not recorded|map legend|||Andamooka. (H53-12).||||||
14329|Nuccaleena Formation|44934|5|Briefly described|Map Legend||Adelaidean|||||||
14329|Nuccaleena Formation|45155|6|Mentioned|p28|||Correlation||||||
14329|Nuccaleena Formation|46865|6|Mentioned|p43|||||||||
14329|Nuccaleena Formation|50327|6|Mentioned|p302, p303, p308|||Within the Adelaide Rift Complex of South Australia. Comparisons mentioned on several pages (see also p305) - refers to correlations with Tasmanian units.||||||07-FEB-11
14329|Nuccaleena 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
14329|Nuccaleena Formation|60889|6|Mentioned|p248 Fig.5|||Top Nuccaleena Fm shown in Fig.5 - Seismic and sequence interpretation in the Moorowie Syncline, below Base Cambrian.||||||
14329|Nuccaleena Formation|60955|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Of the Wilpena Group. Thin red and cream dolomites, dolomite, purple shales.||||||13-APR-05
14329|Nuccaleena Formation|60959|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Of the Sandison Subgroup. Laminated to well bedded, pink, cream to buff-yellow, fine grained dolomicrite. Purple shale interbeds.||||||07-MAR-14
14329|Nuccaleena Formation|61236|5|Briefly described|p24|Adelaidean|Adelaidean|Of Cloud and Glaessner (1982).||||||14-MAY-07
14329|Nuccaleena Formation|61238|4|Described|p46 Fig. 2, p47 Fig. 3|Neoproterozoic|Neoproterozoic|Of the Wilpena Group. Dolomite, thin laminated, micritic, with interbedded shale near top.||||||14-MAY-07
14329|Nuccaleena Formation|61565|5|Briefly described|p609 Fig. 3|Neoproterozoic III|Neoproterozoic III|Geological Province: Adelaide Fold Belt.||||||
14329|Nuccaleena Formation|61732|4|Described|p4 Fig. 3, p41|Marinoan|Marinoan|Of the Sandison Subgroup (Wilpena Group). Gradational contact with Brachina Formation above. Max. thickness: 60m.  Geological Province: Adelaide Rift Complex. See also p5 Tb. 1, p28 Fig. 13, p87.||||||07-FEB-11
14329|Nuccaleena Formation|62085|4|Described|p13-30|Ediacaran|Ediacaran|Marinoan cap carbonate at the base; GSSP for the beginning of the terminal Proterozoic period (Ediacaran).|BASE: 635-632|Lowest part of Wilpena Group.||Overlies Elatina Formation disconformably; is overlain by Brachina Formation.|Glacial cap dolomite, shale.|
14329|Nuccaleena Formation|62453|5|Briefly described|p12 Fig. 8|Ediacaran|Ediacaran|Geological Province: Adelaide Rift Complex/Stuart Shelf.||||||07-MAR-14
14329|Nuccaleena Formation|62516|6|Mentioned|p893|||Comparison of similarities with Cumberland Creel Dolostone made.  Also referred to as a "cap carbonate".||||||
14329|Nuccaleena Formation|62592|5|Briefly described|p50 Table 5.1, p59.|Ediacaran|Ediacaran|Adelaide Geosyncline.||Unit in Sandison Subgroup.||Is overlain by Brachina Formation.|Dolomite, shale.|
14329|Nuccaleena Formation|62903|6|Mentioned|p730 Fig.1|||Presented in figure as Nuccaleena.||||overlies Yerelina Subgroup; is overlain by Brachina Formation||
14329|Nuccaleena Formation|63458|6|Mentioned|p897 Fig.19, p900. |Ediacaran|Ediacaran|||Unit in Wilpena Group.||||
14329|Nuccaleena Formation|63674|6|Mentioned|p18|||Of the Adelaide Fold Belt. Marinoan cap dolostone used as base of Ediacaran System/Period.||||||
14329|Nuccaleena Formation|63762|5|Briefly described|p19|||In S.A.||||||07-FEB-11
14329|Nuccaleena Formation|64068|4|Described|p48|Ediacaran||Flinders Ranges. Sits between Marinoan (Cryogenian) glacials and Cambrian rocks in Enorama Creek, where Ediacaran system and period was formally adopted.|||||Cap carbonate (dolostone) immediately above the Elatina Formation.|05-APR-12
14329|Nuccaleena Formation|64455|5|Briefly described|p137, p139, p140, P138 Fig. 1|Cryogenian|Cryogenian|Of Sandison Subgroup. Overlies Elatina Formation.||||||07-MAR-14
14329|Nuccaleena Formation|64797|6|Mentioned|p153 Fig.2, p164 Fig.11, p169 Fig.12|Ediacaran|Ediacaran|Adelaide Rift Complex. Lithology/rank not shown on diagram.||||||
14329|Nuccaleena Formation|64801|6|Mentioned|p112|Neoproterozoic|Neoproterozoic|||||||
14329|Nuccaleena Formation|65338|6|Mentioned|p64.|Ediacaran|Ediacaran|Flinders Ranges. The base of the Marinoan cap carbonate.||||||
14329|Nuccaleena Formation|65365|5|Briefly described|p10 Fig. 4|Ediacaran|Ediacaran|Adelaide Rift Complex / Stuart Shelf||||||
14329|Nuccaleena Formation|65366|5|Briefly described|p23 Fig. 3|Ediacaran|Ediacaran|Adelaide Rift Complex / Stuart Shelf||||||
14329|Nuccaleena Formation|65410|6|Mentioned|p74.|||Adelaide Geosyncline. Part of Supersequence 3.||||||
14329|Nuccaleena Formation|65644|6|Mentioned|p6, 18|Neoproterozoic|Neoproterozoic|Similar to the 'Cap dolostone' over the Cottons Creek Breccia. Age: Marinoan.||||||27-MAR-12
14329|Nuccaleena Formation|65892|4|Described|p5, p32-34, p36-37, p39. |Ediacaran|Ediacaran|The GSSP of the Ediacaran System was established at the base of this 9m thick Formation in Enorama Creek. Contains acritarch species Skiagia. Contains prominent tepee structures.|c.610 Ma.|Unit in Wilpena Group.||Locally grades into overlying Brachina Formation.|Thick beds of buff, laminated dolomite, overlain by a series of giant straight-crested tepee-ruptured beds, with interbedded dolomites and shales at the top.|27-MAY-15
14329|Nuccaleena Formation|65925|5|Briefly described|Appendix 2.||||||||Dolomite, thin, laminated, micritic, with interbedded shale near the top.|
14329|Nuccaleena Formation|66464|3|Fully described|p165, p167-p177|Ediacaran|Ediacaran|Adelaide Rift Complex. Cap dolostone. 4 lithofacies described in detail. Underlies Brachina Formation, overlies Etina Formation.  ~635 Ma.||||||
14329|Nuccaleena Formation|66569|4|Described|p859, p860, p861 fig.2,|Ediacaran|Ediacaran|Wilpena Group; has the GSSP for Ediacaran System and period; dis- to unconformably overlies Elatina Formation and Yerelina Subgroup; <10 m thick; overlies/intertongues with Seacliff Sandstone; underlies Brachina Formation; mudstone and dolostone at top||||||
14329|Nuccaleena Formation|67030|5|Briefly described|p408, p409 Fig.2, p412 Fig.7 p413 Tb.2|Ediacaran|Ediacaran|Magnetic information presented for comparison (Schmidt et al. 2009). Abbreviated as Nuccaleena Fm in Tb.2 and Fig. 7||||Overlies the Elatina Formation and the Yerelina Subgroup; underlies the Moolooloo Siltstone Member and the Ulupa Siltstone; equivalent to the Seacliff Sandstone.||26-APR-12
14329|Nuccaleena Formation|67484|6|Mentioned|p294 Tb.1, p296|Cryogenian|Cryogenian|Adelaide Rift Complex.||Of the Umberatana Group [?].||Overlain by the Brachina Formation. Underlain by the Elatina Formation.||27-MAY-15
14329|Nuccaleena Formation|67620|5|Briefly described|p5|Cryogenian|Cryogenian|Adelaide Rift Complex.||Umberatana Group.||Overlies Elatina Formation. Is overlain by Brachina Formation (Wilpena Group).||
14329|Nuccaleena Formation|67870|5|Briefly described|p9|Ediacaran|Ediacaran|Adelaide Rift System.||Sandison Subgroup.||||
14329|Nuccaleena Formation|67912|5|Briefly described|p13|Cryogenian|Cryogenian|Flinders Ranges. The GSSP of the Ediacaran System is at the base of this unit.|<635 Ma.|||Overlies Elatina Formation.|Has a cap carbonate at the base.|
14329|Nuccaleena Formation|68030|4|Described|p236-237,239|Ediacaran|Ediacaran|Flinders Ranges. Immediate post-glacial cap carbonate; important lithological marker. See p237 for various interpretations of tepee structures and unit formation mechanisms by various workers. Uppermost red siltstone and shale unit represents a maximum flooding surface. Interbedded with the Seacliff Sandstone Member.||Unit of Wilpena Group.||Lowermost unit of Wilpena Group. Overlain by Brachina Formation. Underlain (locally disconformably) by Enorama Formation, and unconformably by Elatina Formation.|Pink to yellowish dolostone, with purple shale interbeds and lateral sandy facies, grading upwards into red siltstone and shale.|26-JUN-19
14329|Nuccaleena Formation|68138|6|Mentioned|p156|Neoproterozoic|Neoproterozoic|Adelaide Rift Complex.||Umberatana Group.||||
14329|Nuccaleena Formation|68241|5|Briefly described|p16, p19, p29, p30, p32, p33 Fig.3|Ediacaran|Cryogenian|||Of the Adelaide Rift Complex.||Correlative of the Cumberland Creek Dolostone?||26-MAY-17
14329|Nuccaleena Formation|68243|6|Mentioned|p651, p656|||Adelaide Geosyncline. Lithologically and isotopically very similar to the Cumberland Creek Dolostone.||||||
14329|Nuccaleena Formation|68244|6|Mentioned|p671|||Geological province: Adelaide Rift Complex. Chemostratigraphically correlatable to Walsh/Landrigan/Moonlight Valley formations at end Cryogenian glaciation.||||||
14329|Nuccaleena Formation|68269|6|Mentioned|p674|||Adelaide Geosyncline.||Wilpena Group||Underlain by Seacliff Sandstone. Overlain by Brachina Formation.|Dolostone dominated.|
14329|Nuccaleena Formation|68270|6|Mentioned|p679-680, p684|||Correlable to Pioneer Sandstone, Olympic Formation, Wanapi Dolomite Member.||||||03-JUL-19
14329|Nuccaleena Formation|68271|5|Briefly described|p695,697|||Adelaide Rift Complex. Base of the Nuccaleena Formation represents true lower boundary of the stratotypic Ediacaran assemblage.||||Overlain by Ulupa Siltstone. Underlain by Elatina Formation equivalent tillites.||
14329|Nuccaleena Formation|68275|6|Mentioned|p59|||||||Overlies Elatina Formation. Is overlain by Brachina Formation.||
14329|Nuccaleena Formation|68276|6|Mentioned|p71, 75|||The ""Formation"" is omitted.",,|||||Includes cap dolostone; laminated, each lamina representing a sedimentary unit composed of well-sorted, graded or reverse-graded peloids (up to 3mm diameter), terminating with a micropeloidal drape. Sedimentary structures discussed in detail.|
14329|Nuccaleena Formation|68277|6|Mentioned|p102-103, 106|Neoproterozoic|Neoproterozoic|Flinders Ranges. The cap carbonate defines the base of the Ediacaran Period. Paleomagnetism data and inferred tectonic orientations during Ediacaran glaciations discussed.|||||Contains a cap carbonate.|
14329|Nuccaleena Formation|68473|6|Mentioned|p531|||Adelaide Rift Complex.||||||
14329|Nuccaleena Formation|69017|6|Mentioned|p95-98, 101-103|||||||Overlies Elatina Formation. Is overlain by Brachina Formation.|Sandstone, dolostone interfingering with red siltstone, cap-dolostone (described in some detail).|
14329|Nuccaleena Formation|69019|4|Described|p54-55.|Neoproterozoic|Neoproterozoic|Of Coats (in Thomson et al.,1964). Type section is 700 m W of Mt Saturday in the Flinders Ranges. A readily recognisable marker unit, 3-4 m thick throughout much of the Adelaide Geosyncline.||Unit in Sandison Subgroup.||Intertongues with and overlies Seacliff Sandstone.|Pink and cream to buff-yellow dolomicrite that weathers pale yellow-brown, laminated to well-bedded; cyclic purple shale interbeds increasing upsection.|
14329|Nuccaleena Formation|69437|5|Briefly described|p22:7|Ediacaran|Ediacaran|Adelaide Fold Belt. A cap carbonate, marking the base of the Ediacaran period.||||Overlies Elatina Formation.||12-JUL-16
14329|Nuccaleena Formation|69841|5|Briefly described|p7, p19|||The 'cap carbonate' over Elatina Formation.||||Overlies Elatina Formation. Correlative of Cumberland Creek Dolostone.||
14329|Nuccaleena Formation|69873|5|Briefly described|p83|||A cap carbonate: one of a widespread, distinctive, more or less isochronous deposit overlying Marinoan glacials. The base of this unit defines the base of the Ediacaran System.|635 Ma (Hoffmann et al., 2004).|||Overlies Elatina Formation.||
14329|Nuccaleena Formation|70031|5|Briefly described|p245,250-251|Ediacaran|Ediacaran|Adelaide Geosyncline. See p250 Table 2 for paleomagnetic analysis.||Unit of Wilpena Group.||Lowermost unit of Wilpena Group. Overlain by Brachina Formation. Underlain disconformably to unconformably by Elatina Formation/Yerelina Subgroup/Umberatana Group.||
14329|Nuccaleena Formation|70082|5|Briefly described|p2-3,15-16|Ediacaran|Ediacaran|Flinders Ranges, Stuart Shelf and Kulpara-Adelaide region. Contains periglacial paleosols. Global Boundary Stratotype Section and Point (GSSP) and stratotype basal Ediacaran placed base of Nuccaleena Formation. Correlable with Reynella Siltstone Member.||||Overlain disconformably by Seacliff Sandstone.||
14329|Nuccaleena Formation|70333|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic||||||Dolomite, thin, laminated, micritic, with interbedded shale near the top.|
14329|Nuccaleena Formation|70334|4|Described|p2,20,30-32,55-56,65,77|Ediacaran|Ediacaran|Geological province: Gawler Craton. Of Adelaide Geosyncline and Stuart Shelf. Cap dolostone to the Elatina Formation, marking end of Sturtian glaciation; transgressive systems tract. Average thickness: 3m (1-4m). Usually exposed as a prominent marker bed.||Unit of Sandison Subgroup.||Basal unit of Sandison Subgroup. Underlain conformably to unconformably by Elatina Fomation, or Whyalla Sandstone. Intertongued with Seacliff Sandstone.|White-pink to buff poorly-bedded silty dolomite containing green and grey siltstone interbeds containing stylolites and calcite vughs and crosscut by thin calcite veins.|
14329|Nuccaleena Formation|70384|5|Briefly described|Map legend.|Ediacaran|Neoproterozoic|Adelaide Geosyncline. A transgressive succession.||Of Sandison Subgroup.||Unconformably overlies Elatina Formation (Yerelina Subgroup).|Laminated to well-bedded dolomicrite, pink and cream to buff-yellow, weathering to pale yellow-brown. Cyclic purple shale interbeds appear and increase rapidly up-section.|23-JAN-19
14329|Nuccaleena Formation|70406|5|Briefly described|p125, p121, Fig 5|||||Of Sandison Subgroup.||Conformably underlies Brachina Formation. Shown as interfingering with Seacliff Sandstone.||
14329|Nuccaleena Formation|70407|5|Briefly described|p103 Fig 2, p112, 113, 105|Neoproterozoic|Neoproterozoic|Age: Marinoan. Cap dolostone. Associated with sequence boundary.||Of Sandison Subgroup, Wilpena Group.||Overlies Elatina Formation.|Dolostone.|
14329|Nuccaleena Formation|71129|6|Mentioned|p15,117,125-127,129,132,208|Ediacaran|Ediacaran|Of Stuart Shelf and Adelaide Geosyncline. Cap carbonate sequence to the Elatina Formation, deposited during warming and glacio-eustatic sea level rise following Marinoan glaciation.||||Equivalent to Tregolana Shale.||
14329|Nuccaleena Formation|71237|14|Not recorded|p10, 12, 18|||||||||
14329|Nuccaleena Formation|71241|2|Defined|p13,15,  18, p9-10|||||Of Wilpena Group.||||
14329|Nuccaleena Formation|71250|5|Briefly described|p69-70|Ediacaran|Ediacaran|Central Flinders Ranges.||Wilpena Group.||Is overlain by Brachina Formation.|Includes a cap carbonate.|
14329|Nuccaleena Formation|71288|6|Mentioned|p140|Neoproterozoic|Neoproterozoic|||||||
14329|Nuccaleena Formation|71801|6|Mentioned|p231, p238|Ediacaran|Ediacaran||||||Dolostone.|
14329|Nuccaleena Formation|71895|5|Briefly described|p10, APP8. p201-p202, |||Stuart Shelf. See also Nuccaleena Dolomite.||Basal Wilpena Group||Overlain by the Tregolana Shale Member.|Lenticular, white to yellow coloured, thin, laminated, micritic dolomite.|
14329|Nuccaleena Formation|72090|5|Briefly described|p34, p36-p37|||Gawler Craton.|||||Greyish brown, fine- to medium-grained, well sorted, sandstone interbedded with dolomitic shale.|
14329|Nuccaleena Formation|72247|5|Briefly described|p43|Neoproterozoic|Neoproterozoic|Of Adelaide Geosyncline.||Unit of Wilpena Group.||Overlain by Woomera Shale or Tregolana Shale Member. Underlain by Umberatana Group.||
14329|Nuccaleena Formation|72248|6|Mentioned|p147|Ediacaran|Ediacaran|Of Adelaide Geosyncline. Transgressive unit overlying a glaciogenic sequence. Contains aragonitic marine seafloor cements.|c. 600 Ma|||||13-SEP-19
14329|Nuccaleena Formation|72449|5|Briefly described|p1, p2 Map Legend|Neoproterozoic|Neoproterozoic|||||Overlies Elatina Formation and underlies Brachina Formation.|Cream to buff-yellow fine grained dolomite. Purple shale beds appear and increase rapidly upwards.|
14329|Nuccaleena Formation|72450|5|Briefly described|Brochure map|||||Wilpena Group|||Laminated pink dolomite.|
14329|Nuccaleena Formation|72451|6|Mentioned|p4 Fig. 1|Late Proterozoic|Late Proterozoic|Adelaidean age. Appears only in Figure 1.||||||
14329|Nuccaleena Formation|72456|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Marree 1:250k map sheet.|||||Dolomite, thin, laminated, micritic with interbedded shale near the top.|
14329|Nuccaleena Formation|72473|6|Mentioned|p4-6|||Constitutes a widespread marker bed in the Flinders Ranges. A thin (less than 10 m) commonly discontinuously lensed 'cap carbonate' occurs at the base of the unit.|||||Pale reddish dolomite grading to a well-banded reddish fine sandstone.|
14329|Nuccaleena Formation|72613|6|Mentioned|p3|Cryogenian|Cryogenian|Shown as Marinoan age. Northern Flinders Ranges.||||||
14329|Nuccaleena Formation|73086|6|Mentioned|p101, p113, p167|||Adelaide Rift Complex. Marinoan. [May include an informal cap carbonate unit?].||||Correlates to Olympic Formation.||
14329|Nuccaleena Formation|73110|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic||||||Dolomite, thin, laminated, micritic, with interbedded shale near the top.|
14329|Nuccaleena Formation|73188|6|Mentioned|p316|Ediacaran|Ediacaran|Mount Lofty Ranges.||Sandison Subgroup, Wilpena Group|||Pink-buff dolomite.|
14329|Nuccaleena Formation|73226|6|Mentioned|p3|||||||||
14329|Nuccaleena Formation|73227|6|Mentioned|p25, p36|||Adelaide Rift Complex. Marks the end of the Marinoan glacial episode and the base of the Ediacaran. May have acted as a caprock for mineralizing fluids in the underlying Whyalla Sandstone.||Wilpena Group||Underlain by Whyalla Sandstone. Overlain by 'Woomera Shale' and Tregolana Shale Member (Tent Hill Formation).|Includes dolomite.|
14329|Nuccaleena Formation|73234|6|Mentioned|p6, p20|Ediacaran|Cryogenian|Post glacial.|c. 635 Ma|||Overlain by Tent Hill Formation (Wilpena Group).|Dolomitic.|
14329|Nuccaleena Formation|73236|4|Described|p36-39, p45, p47|Ediacaran|Ediacaran|Marine shelf sedimentary rocks. Occurs as lenses interfingering with the Seacliff Sandstone at Hallett Cove. Transgressively overlie Marinoan-aged glacials in the Flinders Ranges.||Sandison Subgroup, Wilpena Group, Heysen Supergroup||Conformably underlain by and interfingers with Seacliff Formation. Conformably overlain by Brachina Formation.|Pink to buff, well-laminated, fine-grained dolomite with red shale partings.|
14329|Nuccaleena Formation|73255|5|Briefly described|p534-535, p546, p549|Ediacaran|Ediacaran|Cap carbonate'.||||Overlies the Elatina Formation, underlies the Brachina Formation.|Partly eolian deposit of dolomite, quartz and feldspar capping a thick red tillite.|
14329|Nuccaleena Formation|74367|6|Mentioned|p7 Fig.6|||||Sandison Subgroup||||
14374|Nullawarre Greensand|12796|4|Described|p460, p456 Fig. 2|Santonian|Santonian|Of Sherbrook Gp. Originally basal member of Paarratte Fm. Fine-coarse-grained sandstone of quartz grains and glauconite pellets. Interfingering and overlying Belfast Mdst; underlies Skull Creek Mdst. Geol. Prov: Otway Basin/Port Campbell Embayment.||||||
14374|Nullawarre Greensand|22470|5|Briefly described|p13 Fig. 17|Santonian|Santonian|Of Sherbrook Group.||||||
14374|Nullawarre Greensand|22674|5|Briefly described|Fig.2 p719|Campanian|Santonian|||||||
14374|Nullawarre Greensand|22875|3|Fully described|p44|Late Cretaceous|Late Cretaceous|Of the Sherbrook Group.||||||26-SEP-07
14374|Nullawarre Greensand|22944|5|Briefly described|Fig3|||||||||
14374|Nullawarre Greensand|24551|6|Mentioned|p257 Fig. 9.25|||Of the Sherbrook Group.||||||04-FEB-08
14374|Nullawarre Greensand|24562|5|Briefly described|p6, 8 Fig. 2|Late Cretaceous|Late Cretaceous|Of the Sherbrook Group.  Geological Province: Otway Basin.||||||
14374|Nullawarre Greensand|30578|5|Briefly described|p7|||||||||
14374|Nullawarre Greensand|30580|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
14374|Nullawarre Greensand|30932|6|Mentioned|Map legend|Late Cretaceous|Late Cretaceous|Part of Paaratte Formation.||||||04-FEB-08
14374|Nullawarre Greensand|31424|6|Mentioned|Fig.2|||||||||
14374|Nullawarre Greensand|36913|6|Mentioned|Fig.2|||||||||
14374|Nullawarre Greensand|41016|5|Briefly described|Table 1|||||||||
14374|Nullawarre Greensand|41185|6|Mentioned|p177|||||||||
14374|Nullawarre Greensand|41642|4|Described|p244|||||||||
14374|Nullawarre Greensand|41704|6|Mentioned|Fig.3|||||||||
14374|Nullawarre Greensand|41868|6|Mentioned|p533|||||||||
14374|Nullawarre Greensand|42524|5|Briefly described|Fig.3 P27|||||||||
14374|Nullawarre Greensand|42555|5|Briefly described|p285|||||||||
14374|Nullawarre Greensand|42863|5|Briefly described|Fig.14|||Variation on Victorian unit.||||||
14374|Nullawarre Greensand|43171|6|Mentioned|5|||Of Sherbrook Formation||||||
14374|Nullawarre Greensand|43208|5|Briefly described|map legend|Campanian|Santonian|Of Sherbrook Group.||||||
14374|Nullawarre Greensand|43590|4|Described|p14|Campanian|Santonian|||||||
14374|Nullawarre Greensand|43660|6|Mentioned|Fig.6,p15||Late Cretaceous|||||||
14374|Nullawarre Greensand|43744|6|Mentioned|Fig.3,p3|||||||||
14374|Nullawarre Greensand|43937|5|Briefly described|Map Legend|Santonian|Aptian|||||||
14374|Nullawarre Greensand|61017|5|Briefly described|p5 Fig. 2|Santonian|Santonian|Of the Sherbrook Group. Geological Province: Otway Basin. See also p6 Fig. 3.||||||07-FEB-11
14374|Nullawarre Greensand|61182|3|Fully described|p17-18, p31, p88|Campanian|Santonian|Of Sherbrook Gp. Conformably overlies/interfingers with Belfast Mudstone; conformably overlain by Paaratte Fm. Max. thickness: ~130m. Geol.Prov: Otway Basin. Light greenish-grey, fine- to coarse-gr. sandstone. Formerly regarded as part of Paarratte Fm.||||||
14374|Nullawarre Greensand|61230|6|Mentioned|p319 Fig.2.|Santonian|Coniacian|||Unit in Sherbrook Group.||||
14374|Nullawarre Greensand|61470|5|Briefly described|p28 Fig. 5|Santonian|Santonian|Of the Sherbrook Group. Overlies and interfingers with Belfast Mudstone; underlies Skull Creek Mudstone. Geological Province: Otway Basin.||||||12-OCT-05
14374|Nullawarre Greensand|61625|5|Briefly described|p475, p476 Fig. 1, p477, p480, p483|Late Creatceous|Late Cretaceous|Of Sherbrook Group. Geological Province: Otway Basin. Coarsening upward profile of fine- very coarse-grained glaconitic sandstone.||||||07-FEB-11
14374|Nullawarre Greensand|61628|5|Briefly described|p509 Fig. 3|Late Cretaceous|Late Cretaceous|Of Sherbrook Group. Geological Province: Otway Basin.||||||31-MAR-09
14374|Nullawarre Greensand|63124|5|Briefly described|p48 Fig. 5.1|||Previously Nullawarre Greensand Member (Sprigg 1986) as a member of his Paaratte Formation; elevated to formation status by Williamson et al (1987). Interfingers with Belfast Mudstone representing a shelf equivalent. Geological Province: Otway Basin.||||||
14374|Nullawarre Greensand|63269|5|Briefly described|p605|Late Cretaceous|Late Cretaceous|Otway Basin.||Sherbrook Group.||||
14374|Nullawarre Greensand|66245|5|Briefly described|p6 Fig.5. |Campanian|Santonian|||Unit in Sherbrook Group.||Is intercalated with Belfast Mudstone and Paaratte Formation.||
14374|Nullawarre Greensand|67061|6|Mentioned|p546 Fig.3.|Late Cretaceous|Late Cretaceous|||Unit in Sherbrook Group.||||
14374|Nullawarre Greensand|67367|5|Briefly described|p131 Fig.2. |Late Cretaceous|Late Cretaceous|||Unit in Sherbrook Group.||||
14374|Nullawarre Greensand|69297|5|Briefly described|p79, p98|Santonian|Santonian|Otway Basin.||Sherbrook Group||Overlies the Belfast Mudstone. Overlain by the Skull Creek Mudstone.|Mudstone and greensand.|
14374|Nullawarre Greensand|69651|5|Briefly described|p10|Late Cretaceous|Late Cretaceous|||Sherbrook Group.||Is interbedded with Belfast Mudstone and Paaratte Formation.||
14374|Nullawarre Greensand|70077|5|Briefly described|Nelson: Fig.2. Regional: Fig.4|Santonian|Santonian|Otway Basin: Port Campbell Embayment.||Sherbrook Group.||Overlies Belfast Mudstone. Is overlain by Skull Creek Mudstone.||
14374|Nullawarre Greensand|70193|6|Mentioned|p284 Fig 2, p285 fig 3|Santonian|Santonian|Geological province: Otway Basin. Part of the Sherbrook Supersequence.||||||
14374|Nullawarre Greensand|70880|6|Mentioned|p77|Santonian|Santonian|Otway Basin.||||||
14374|Nullawarre Greensand|71266|6|Mentioned|p614 Fig.3|Late Cretaceous|Late Cretaceous|Otway Basin.||||||
14374|Nullawarre Greensand|71437|6|Mentioned|p157|Late Cretaceous|Late Cretaceous|Abbreviation of Nullawarre Greensand Member.||Of Paaratte Formation.||||
14374|Nullawarre Greensand|73357|5|Briefly described|p21, p31, p45|Santonian|Santonian|Otway Basin. Correlated with the Isabelidinium cretaceum Dinocyst Zone and Tricolpites apoxyexinus Spore-Pollen Zone.||Of Sherbrook Group.||Overlies Belfast Mudstone, underlies Skull Creek Mudstone.||
14374|Nullawarre Greensand|73383|5|Briefly described|p3, p10 Tb.3.7, p21-22, p27, p200, p261|Santonian|Santonian|Otway Basin. Approximately equivalent to chemostratigraphic package S5-P5, defined by high Fe, P, Th/K and Sm/U values. Attributed to berthierine or glauconite, and phosphate cements. Lithologies based on geochemistry using the ChemLith classification includes argillaceous sandstone, and using the Herron classification (1988) includes Fe-sand and quartz arenite. See also vi, p11 Tb.3.9, p67-68, p133-134.||Sherbrook Group||Overlies Belfast Mudstone, underlies Skull Creek Mudstone, Paaratte Formation|Shallow marine and nearshore sandstones.|
14374|Nullawarre Greensand|73385|5|Briefly described|p5|Santonian|Santonian|Otway Basin.||Sherbrook Group||Overlies Belfast Mudstone, underlies Skull Creek Mudstone, Paaratte Formation.|Shallow marine and nearshore sandstones.|
14374|Nullawarre Greensand|73386|4|Described|p4, p6, p10-11, Attachment A1|Santonian|Santonian|Otway Basin. Originally described as part of the Paaratte Formation. Type section is defined between 1344 m and 1514 m in Nullawarre-3. Shallow marine depositional environment, represents progradation of marine upper deltaic, nearshore, beach-barrier facies. Top of unit is a regional maximum flooding/transgressive surface. Occurs with the Tricolporites apoxyexinus Spore-Pollen Zone. Predominantly restricted to Port Campbell and Tyrendarra embayments.||Sherbrook Group||Overlies Belfast Mudstone, conformably underlies Skull Creek Mudstone, underlies Paaratte Formation|Distinctive grey-green, glauconitic, fine- to coarse-grained sandstone.|
14374|Nullawarre Greensand|73594|5|Briefly described|p4-5, p31|Santonian|Santonian|Otway Basin. Shallow marine.||Sherbrook Group||Overlies Flaxman Formation, Belfast Mudstone, underlies Skull Creek Mudstone, Paaratte Formation|Glauconitic sandstones.|
14413|Nurragi Clay|38290|2|Defined|p43|Quaternary|Quaternary|||||||
14485|Observatory Hill Formation|22613|5|Briefly described|p17|Neoproterozoic|Neoproterozoic|||||||
14485|Observatory Hill Formation|22746|5|Briefly described|Fig.3 p515|Early Cambrian|Early Cambrian|||||||
14485|Observatory Hill Formation|22917|6|Mentioned|10|||||||||
14485|Observatory Hill Formation|22922|6|Mentioned|34|||Underlying unit Relief Sandstone||||||
14485|Observatory Hill Formation|23282|2|Defined|p72||Early Cambrian|Age: Early Cambrian 524 - 520Ma. of Marla Group, Officer Basin. Introduced by Wopfner (1969) as 'Observatory Hill Beds', & designated a Formation by Brewer et al. (1987).||||||01-APR-14
14485|Observatory Hill Formation|23288|6|Mentioned|Fig.5||Early Cambrian|||||||
14485|Observatory Hill Formation|23479|5|Briefly described|p26|Paleozoic|Paleozoic|Of Marla Group. Geological Province: Gawler Craton.||||||07-NOV-08
14485|Observatory Hill Formation|23524|5|Briefly described|p221 Fig. 3|Early Cambrian|Early Cambrian|||||||
14485|Observatory Hill Formation|23981|5|Briefly described|p10 Fig. 5|Toyonian|Toyonian|Geological Province: eastern Officer Basin.||||||15-FEB-07
14485|Observatory Hill Formation|24112|5|Briefly described|p254 Fig.2|Early Cambrian|Early Cambrian|Of the Marla Group. Geological Province: Officer Basin||||||
14485|Observatory Hill Formation|40945|1|Redefined|p3|Middle Cambrian|Early Cambrian|Previously named as Observatory Hill Beds||||||
14485|Observatory Hill Formation|41609|6|Mentioned|p131|||||||||
14485|Observatory Hill Formation|42065|5|Briefly described|p185|||See also Fig.2||||||
14485|Observatory Hill Formation|42095|5|Briefly described|Fig.3 P31|||||||||
14485|Observatory Hill Formation|42096|6|Mentioned|p36|||||||||
14485|Observatory Hill Formation|42816|4|Described|p14|||||||||
14485|Observatory Hill Formation|43052|5|Briefly described|Table 2.1|||||||||
14485|Observatory Hill Formation|43053|5|Briefly described|Map Legend|Cambrian|Cambrian|Of the Marla Group. Playa siltstone, shale, carbonate and chert.||||||25-MAY-05
14485|Observatory Hill Formation|43258|5|Briefly described|Map Legend||Cambrian|||||||
14485|Observatory Hill Formation|43298|5|Briefly described|Map Legend||Cambrian|||||||
14485|Observatory Hill Formation|43650|6|Mentioned|Fig.2,p444|||||||||
14485|Observatory Hill Formation|43732|4|Described|p3||Cambrian|||||||
14485|Observatory Hill Formation|43743|6|Mentioned|Fig.2,p33||Early Cambrian|||||||
14485|Observatory Hill Formation|44109|5|Briefly described|p22 Fig. 19|Cambrian|Cambrian|Of the Marla Group. Geological Province: central Officer Basin.||||||
14485|Observatory Hill Formation|44111|6|Mentioned|p.58, Fig. 2|||Officer Basin. presented as "Observatory Hill" only in Fig. 2.||||||
14485|Observatory Hill Formation|44133|5|Briefly described|p37, 4 Fig. 7.2|Middle Paleozoic|Early Paleozoic|Geological Province: Eastern Officer Basin. Of the Marla Group.||||||07-NOV-08
14485|Observatory Hill Formation|60565|5|Briefly described|p116, p18, p20 Fig.3b|Cambrian|Cambrian|Mainly fluvial-lacustrine red-brown siltstone and alkaline playa siliciclastic-carbonate deposits. Geological Province: Officer Basin.||||||02-MAY-13
14485|Observatory Hill Formation|60953|5|Briefly described|Map Legend|Cambrian|Cambrian|Playa siltstone, shale, carbonate and chert; fluvial arkose and fanglomerate.||||||
14485|Observatory Hill Formation|61108|5|Briefly described|map legend|Cambrian|Cambrian|Playa siltstone, shale, carbonate and chert.||||||
14485|Observatory Hill Formation|61732|5|Briefly described|p67, p78|Cambrian|Cambrian|Of the Marla Group. Unconformably overlies Wilari Dolomite Member (Tanana Formation).||||||07-FEB-11
14485|Observatory Hill Formation|62570|5|Briefly described|p579, p580 Figs. 2 and 3|Early Cambrian|Early Cambrian|Of the Marla Gp. Includes 5 members. Conformably overlies Ouldburra Formation. Geol.Prov: Officer Basin. Carbonates. Alternates between siltstone redbed, fluvial and alkaline playa deposits. Max. thickness: 400m.||||||01-OCT-09
14485|Observatory Hill Formation|63397|6|Mentioned|9|Cambrian|Cambrian|||||||
14485|Observatory Hill Formation|65194|5|Briefly described|p167|||Underlying formation in Officer Basin.||||||
14485|Observatory Hill Formation|65313|5|Briefly described|p577, p578 Fig. 6|Middle Cambrian|Early Cambrian|Marla 1 well and Observatory Hill section, Officer Basin. Contains Early Cambrian trilobites.||Of Marla Group.|Includes Arcoeillinna, Oolarinna, Moyles Creek Chert, Parakeelya Alkali, and Wallatinna Members.|Underlies Apamurra Formation.||26-MAR-12
14485|Observatory Hill Formation|65416|6|Mentioned|p146.|||Suggested by Perincek (1996) to post-date the Petermann Ranges Orogeny.||||||
14485|Observatory Hill Formation|67120|5|Briefly described|Map legend|Cambrian|Cambrian|||Marla Group|||Siltstone and claystone, micaceous, calcareous and dolomitic in part; minor sandstone; limestone and dolomite. Minor chert.|
14485|Observatory Hill 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.|
14485|Observatory Hill Formation|67912|5|Briefly described|p13-14|Ediacaran|Ediacaran|Eastern Officer Basin. Subsurface; penetrated by the Lake Maurice West 1 drillhole where it is 206.3m thick.||||Overlies Ungoolya Group.||
14485|Observatory Hill Formation|67921|5|Briefly described|Map legend|Cambrian|Cambrian|Grouped with Wirrildar beds and Arcoeillina Sandstone. Group description: Fluvial, lacustrine, aeolian and sabkha deposits including micaceous and feldspathic sandstone and mudstone, cherty (Magadi-type) siltstone and carbonate interbeds.||||Grouped with Arcoeillina Sandstone, Wirrildar beds||
14485|Observatory Hill Formation|69648|6|Mentioned|p18, p19|||Lithologies originally interpreted as Cambrian Observatory Hill Formation in SADME Ooldea 3 have been tentatively correlated with Meramangye Formation on OOLDEA map sheet. See Observatory Hill Beds and Mermangye Formation.||||||
14485|Observatory Hill Formation|69946|6|Mentioned|p38|||||||Conformably overlies Ouldburra Formation. Is overlain unconformably by Boorthanna Formation.||
14485|Observatory Hill Formation|70336|5|Briefly described|Map legend|Cambrian|Cambrian|||Marla Group.|||Siltstone and claystone, micaceous, calcareous and dolomitic in part; minor sandstone, limestone and dolomite. Minor chert.|
14485|Observatory Hill Formation|71342|6|Mentioned|Ch5 p38|Cambrian|Cambrian|Arckaringa Basin.||||Overlies the Ouldburra Formation. Unconformably overlain by the Boorthana Formation.||
14485|Observatory Hill Formation|72478|6|Mentioned|p8, p9|Cambrian|Cambrian|Officer Basin. Shown as Observatory Hills Beds p11, digital p69. See also p51, 70 [of the document].||Marla Group|Includes the Wallatinna Member, Parakeelya Alkaki Member, Moyles Chert Marker Bed, Oolarinna Member.|||29-MAR-21
14485|Observatory Hill Formation|73090|5|Briefly described|p12 Fig.7, Appendix|Cambrian|Cambrian|||Marla Group.|||Siltstone and claystone, micaceous, calcareous and dolomitic in part; minor sandstone; limestone and dolomite. Minor chert.|
14485|Observatory Hill Formation|73099|5|Briefly described|Map legend.|Middle Cambrian|Early Cambrian|Officer Basin.||Marla Group.|Cadney Park, Parakeelya Alkali, Oolarinna Members; Moyles Chert Marker Bed.|Overlies Relief Sandstone. Is overlain by Arcoeillinna Sandstone.|Undifferentiated alluvial, lacustrine and alkaline playa sediments.|
14485|Observatory Hill Formation|73100|5|Briefly described|Map legend|Cambrian|Cambrian|Subsurface. Mapped as one unit with Arcoeillina Sandstone and Wirrildar beds.||||||
14485|Observatory Hill Formation|73111|5|Briefly described|Map legend.|Cambrian|Cambrian|Mapped as one unit with Arcoeillina Sandstone and Wirrildar beds. Subcrop and minor outcrop.|||||Fluvial, lacustrine, aeolian and sabkha deposits including micaceous and feldspathic sandstone and mudstone, cherty (Magadi-type) siltstone and carbonate interbeds.|
14485|Observatory Hill Formation|73392|6|Mentioned|p3||||||||Sampled from core of Giles 1 well, Munta 1, Birksgate 1 wells.|
14490|Ochre Cove Formation|22525|4|Described|p38,39||Pleistocene|sometimes combined with overlying Seaford Formation as the Robinson Point Formation (old usage)||||||
14490|Ochre Cove Formation|22941|5|Briefly described|p290|||||||||
14490|Ochre Cove Formation|23489|4|Described|p46|Pleistocene|Pleistocene|Max. thickness: 8 m.||||||
14490|Ochre Cove Formation|24102|5|Briefly described|p132 Fig.2|Quaternary|Quaternary|Age: ~780 Ka.||||||30-NOV-04
14490|Ochre Cove Formation|24566|6|Mentioned|p110|||||||||
14490|Ochre Cove Formation|35097|6|Mentioned|Fig.4|||||||||
14490|Ochre Cove Formation|35689|6|Mentioned|Plate 7|||||||||
14490|Ochre Cove Formation|36127|6|Mentioned|p11|||See also P7.||||||
14490|Ochre Cove Formation|38290|6|Mentioned|p55|||||||||
14490|Ochre Cove Formation|39351|6|Mentioned|Map legend|Quaternary|Quaternary|||||||
14490|Ochre Cove Formation|39522|6|Mentioned|p85|||||||||
14490|Ochre Cove Formation|41495|4|Described|p44|||||||||
14490|Ochre Cove Formation|41513|5|Briefly described|Fig.5|||||||||
14490|Ochre Cove Formation|41551|6|Mentioned|p463|||||||||
14490|Ochre Cove Formation|43682|5|Briefly described|p290|||||||||
14490|Ochre Cove Formation|44198|2|Defined|p31|Early Pleistocene|Early Pleistocene|||||||
14490|Ochre Cove Formation|44199|2|Defined|p594 - 597|Quaternary|Neogene|late Tertiary - Quaternary. Alluvial.||||||
14490|Ochre Cove Formation|44200|6|Mentioned|p.352, 355.|||||||||
14490|Ochre Cove Formation|61155|5|Briefly described|p17|Pleistocene|Pleistocene|Overlies Burnham Limestone and Hindmarsh Clay. Geological Province: St Vincent Basin.||||||
14490|Ochre Cove Formation|64705|5|Briefly described|p80 Fig. 7e (photo)|Quaternary|Quaternary|Age: ~780,000a.||||||04-DEC-08
14490|Ochre Cove Formation|65901|4|Described|p176, p176 Tab.1, p178 Fig.2|Calabrian|Pleistocene|Red and orange iron-mottled sandy sediment. Contains Jaramillo geomagnetic subchron of ~900 ka and Brunhes/Matuyama geomagnetic reversal of 780 ka.||Included in Hindmarsh Clay by Firman (1967).||Overlies Kurrajong Formation. Overlain by Taringa Formation.|Red and orange iron-mottled sandy sediment.|08-MAR-12
14490|Ochre Cove Formation|66194|5|Briefly described|p580, p587|Pleistocene|Pleistocene|Mid-Pleistocene date (range of at least 1.07 Ma - 780ka) from paleomagnetic dating.||||Overlies the Kurrajong Formation.|Red and grey angular gravels and conglomerates with some layers of strongly mottled clays.|09-MAR-12
14490|Ochre Cove Formation|70660|5|Briefly described|p3, p9-p12, p20 fig 11a|Middle Pleistocene|Middle Pleistocene|See also p21 fig 11c, p29-p30, p32, p37, p40-p41.||||Overlies the Burnham Limestone. Overlain by the Ngaltinga Formation and the Christies Beach Formation.|Sands and gravels, strongly mottled in reds.|
14490|Ochre Cove Formation|72450|6|Mentioned|Brochure, Brochure map|Pleistocene|Pleistocene|Crops out in the coastal cliffs at Ochre Point and Blanche Point. Exposed inland at the road cut on Old Coach Road, north of Aldinga, in upper benches in the Rocla and Hanson sand pits at Maslin Beach.||||Unconformably underlies Pirramimma Sandstone.|Red and yellow, mottled, coarse-grained sandstone.|
14490|Ochre Cove Formation|73188|5|Briefly described|[See comments]|Pleistocene|Pleistocene|St Vincent Basin. Affected by ferruginisation and local silicification. May interfinger with Hindmarsh Clay. Alluvial fan setting adjacent to fault scarps. p: 314, 319-320, 331, 333-335, 337-338, 345-346, 349-351, 356, 358-359.||||Disconformably underlain by Seaford Formation. Unconformably underlain by Bunyeroo Formation and ABC Range Quartzite. Overlain by Ngaltinga Clay[Formation].|Channel cross-bedded sandstone and gravel including ferruginised conglomerate, grit and sandstone.|
14490|Ochre Cove Formation|73236|4|Described|p36, p38, p42-43, p48|Pleistocene|Pleistocene|Fluvial channel sediments. Lenticular beds. Pebbles are derived from the Wilmington Formation in the Mount Lofty Ranges.|c. 2-0.13 Ma|||Underlain by Hallett Cove Sandstone, Burnham Limestone, and Cape Jervis Formation. Overlain by Hindmarsh Clay.|Ferruginised conglomerate of siltstone and sandstone pebbles.|
14512|Olary Alkaline Pyroclastics|40811|4|Described|p319|||||||||
14547|Olia Gneiss|22716|5|Briefly described|table4, p237|Mesoproterozoic|Mesoproterozoic|Age: 1600 Ma.||||||
14547|Olia Gneiss|22826|4|Described|p567|Neoproterozoic|Neoproterozoic|The Olia Gneiss forms the basement to the Amadeus Basin in the south together with the Musgrave-Mann Complex. It is intruded by Granite and by dolerite dykes; overlain unconformably by the Dean Quartzite.||||||03-AUG-09
14547|Olia Gneiss|23483|5|Briefly described|p4|||||||||
14547|Olia Gneiss|23818|6|Mentioned|p43|||||||||
14547|Olia Gneiss|24197|5|Briefly described|p97|||Amphibolite-facies gneisses north of Woodroffe Thrust (Mulga Park Domain). Geological Province: Musgrave Block.||||||07-FEB-11
14547|Olia Gneiss|24496|5|Briefly described|p14|Paleoproterozoic|Paleoproterozoic|May be protolith for some Pottyu Suite granitoids. Geological Province: Musgrave Block.||||||10-JUL-13
14547|Olia Gneiss|24499|5|Briefly described|Map legend|||||||||
14547|Olia Gneiss|30815|6|Mentioned|Map legend|Precambrian|Precambrian|||||||
14547|Olia Gneiss|30817|5|Briefly described|p14|||Age of metamorphism discussed.||||||
14547|Olia Gneiss|33468|6|Mentioned|p214|||Metamorphic equiv.||||||
14547|Olia Gneiss|33478|5|Briefly described|p451|||||||||
14547|Olia Gneiss|34537|6|Mentioned|p43|||||||||
14547|Olia Gneiss|35102|6|Mentioned|p1|||||||||
14547|Olia Gneiss|35308|5|Briefly described|p451|||||||||
14547|Olia Gneiss|36473|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
14547|Olia Gneiss|36887|5|Briefly described|p208|||||||||
14547|Olia Gneiss|40740|6|Mentioned|p1|||||||||
14547|Olia Gneiss|41723|6|Mentioned|Map legend|Paleoproterozoic||||||||07-NOV-08
14547|Olia Gneiss|42504|6|Mentioned|p67|||||||||
14547|Olia Gneiss|42794|6|Mentioned|p3|||||||||
14547|Olia Gneiss|42844|6|Mentioned|p469|||||||||
14547|Olia Gneiss|42940|5|Briefly described|Plate 2|Mesoproterozoic|Paleoproterozoic|Gneiss, granite, schist.  Geological province: Musgrave Block.||||||07-NOV-08
14547|Olia Gneiss|43053|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Metasediments, gneiss, granulite. Geological Province: Musgrave Block.||||||07-NOV-08
14547|Olia Gneiss|43258|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
14547|Olia Gneiss|43298|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
14547|Olia Gneiss|43697|6|Mentioned|p27|||||||||
14547|Olia Gneiss|44109|5|Briefly described|p164, p157|Mesoproterozoic|Mesoproterozoic|Age: <1600Ma. See also p165 Fig. 163C and p166 Fig. 164.||||||
14547|Olia Gneiss|44139|5|Briefly described|p283, 285 Fig. 3-69, p286|||Wells et al. (1970). Of Wingelina Complex. Fine- to medium-grained banded quartzofeldspathic gneiss, and intrusions of porphyritic granite; all at amphibolite facies. Occurs in northern Wingelina Complex below Woodroffe Thrust. Unconformably overlain by Dean Quartzite.|| ||||06-MAR-18
14547|Olia Gneiss|44493|4|Described|p.7, map||Precambrian|BLOOD RANGE sheet (G53-3).||||||21-NOV-06
14547|Olia Gneiss|44494|14|Not recorded|map legend||Precambrian|Undifferentiated.||||||
14547|Olia Gneiss|44495|4|Described|p.4,5, map||Precambrian|AYERS ROCK sheet (G52-8). See p.7,9, for details.||||||21-NOV-06
14547|Olia Gneiss|44496|5|Briefly described|map legend||Precambrian|Gneiss with schist, porphyroblastic schist, amphibolite, migmatite and granite.||||||10-JUL-13
14547|Olia Gneiss|45041|5|Briefly described|p14|||Precamb. Refers Forman (1966)||||||
14547|Olia Gneiss|45085|6|Mentioned|p14|||Age of metamorphism.||||||
14547|Olia Gneiss|45170|6|Mentioned|p5|||||||||
14547|Olia Gneiss|48864|2|Defined|p.17,18||Neoproterozoic|Tb.1. On many pages. p.16,22,28,29,33,39,41,42,44,52,Pl.9,11-13, (G52-3,7,8).late U.Prot.||||||
14547|Olia Gneiss|48963|6|Mentioned|p3|||||||||
14547|Olia Gneiss|49833|6|Mentioned|p8|||||||||
14547|Olia Gneiss|50607|5|Briefly described|p1.1, 2.2|||Geological Province: Musgrave Block. Of the Kulgera Supersuite.||||||
14547|Olia Gneiss|60662|5|Briefly described|Map legend|||Layered to massive amphibolite facies gneisses.||||||22-FEB-05
14547|Olia Gneiss|60683|5|Briefly described|p55 Appendix|||Originally of Forman (1966a, 1972).  Replaced by Umutju Granite Suite (Matapayika Granite), Pottoyu Granite Suite (Mulyatti Granite) and Mantarurr Granite Suite (Kulu, Foster Cliff and Wala Wuru Granites). Overlain by Bloods Range beds and Dean Quartzite.||||||
14547|Olia Gneiss|60953|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Age: >1607Ma (metamorphic age). Amphibolite facies gneiss, minor pelitic schist.||||||07-NOV-08
14547|Olia Gneiss|61108|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|Gneiss, amphibolite-facies; minor pelitic schist. Age: >1607 Ma (metamorphic age).||||||07-NOV-08
14547|Olia Gneiss|61154|6|Mentioned|p4|||See also "Olia Gneiss".||||||
14547|Olia Gneiss|61306|6|Mentioned|p61|||Geological Province: Amadeus Basin.||||||
14547|Olia Gneiss|62609|5|Briefly described|Map Legend|Precambrian|Precambrian|Gneiss, granite, schist.||||||
14547|Olia Gneiss|62620|5|Briefly described|Map Legend|Precambrian|Precambrian|Gneiss, granite, schist.||||||
14547|Olia Gneiss|64745|5|Briefly described|p373 Fig. 3|||Included within informal Musgravian Gneiss in this paper. Geol. Prov: Mulga Park Domain, Musgrave Province. See Olia gneiss.||||||
14547|Olia Gneiss|65376|6|Mentioned|p9 Fig.1.2. |Paleoproterozoic|Paleoproterozoic|||||||
14547|Olia Gneiss|67536|6|Mentioned|Map Legend|||Musgrave Block. Informally subdivided into three parts.|||||Altered, sheared, demagnetised gneiss adjacent to major shear zones, weakly magnetic; layered gneiss, moderately to strongly magnetic; massive or poorly-banded gneiss, moderately magnetic.|
14547|Olia Gneiss|68100|5|Briefly described|p6 |||Of Major and Conor (1993). Mulga Park Domain. Not correlated with Birksgate Complex. Ages of granitic protoliths up to 1591 Ma.|||||Orthogneiss, paragneiss, gneisses, often with granitic protoliths.|19-JAN-17
14547|Olia Gneiss|68131|5|Briefly described|p2 Fig.1|Paleoproterozoic|Paleoproterozoic||||||Gneiss.|
14547|Olia Gneiss|69926|6|Mentioned|p156|||Forman (1972). Eastern Musgrave Block.|||||Amphibolite facies rocks.|
14547|Olia Gneiss|70083|6|Mentioned|p206|||The name used for the Musgravian Gneiss in the Mulga Park Subdomain, Eastern Musgrave Inlier, Musgrave-Albany-Fraser Orogen. Is termed the Birksgate Complex in the Fregon Subdomain.||||||
14547|Olia Gneiss|71210|6|Mentioned|p3, p7|||||||||
14547|Olia Gneiss|71211|6|Mentioned|p228|Mesoproterozoic|Mesoproterozoic|Metamorphosed at 1220-1150 Ma during the Musgravian Orogeny.|1600-1540 Ma||||Felsic gneiss with interlayered and subordinate mafic units and rare metapelite.|
14553|Olney Formation|2967|5|Briefly described|p14, p15 Fig.2.2, p20|||Lawrence (1975). Murray Basin. Lacustrine and paludal sediments.||Renmark Group.||Overlies Warina Sand. Is overlain by Ettrick Marl, Geera Clay and Calivil Formation.|Carbonaceous silt, with additional clays, claystones, coals and sand.|
14553|Olney Formation|10010|5|Briefly described|p12 Fig. 3|Early Miocene|Early Eocene|Overlies Renmark Group. Geological Province: Murray Basin.||||||13-AUG-07
14553|Olney Formation|22587|6|Mentioned|p79 Fig.7|Early Miocene|Middle Eocene|||||||
14553|Olney Formation|22773|5|Briefly described|p340,351,Fig24.8p352|Oligocene|Eocene|||||||
14553|Olney Formation|22799|2|Defined|p28|Middle Miocene|Eocene|||||||
14553|Olney Formation|22857|5|Briefly described|p351, p352 Fig.24.8|Miocene|Early Eocene|Of the Renmark Group. Lithologically variable carbonaceous silts. Sands and clay; local coal and lignite. Overlies the basal Warina Sand. Age: <60Ma. Max. thickness: 300m. Geological Province: Murray Basin. See also p353 Fig. 24.9.||||||
14553|Olney Formation|22887|2|Defined|p33, Fig.6 p13|Middle Miocene|Early Eocene|Probably equivalent to upper 'Renmark beds'.||||||03-FEB-09
14553|Olney Formation|22893|3|Fully described|p25-28|Middle Miocene|Middle Eocene|||||||
14553|Olney Formation|22971|4|Described|p 26|Miocene|Eocene|Of the Renmark Group.||||||25-MAR-08
14553|Olney Formation|23234|6|Mentioned|p88|||||||||
14553|Olney Formation|23252|5|Briefly described|Map Legend||Tertiary|Of Renmark Group. The main basal unit for the Bolligal sheet area. Informally divided into Upper, Middle and Lower Olney Formation.||||||25-MAR-08
14553|Olney Formation|23884|5|Briefly described|p155 Fig.13.2|Middle Miocene|Early Eocene|Geological Province: Murray Basin. Of the Renmark Group.||||||
14553|Olney Formation|23921|5|Briefly described|p1114|Middle Miocene|Middle Miocene|Geological Province: Murray Basin.  See also upper Renmark Group beds.||||||
14553|Olney Formation|24105|5|Briefly described|p158|Miocene|Late Eocene|Geological Province: Murray Basin. Underlying Unit: Warina Sand.||||||
14553|Olney Formation|24177|5|Briefly described|p14, p69|Neogene|Paleogene|Of the Renmark Group. Overlies the Warina Sand. Age: ~45Ma. Geological Province: Murray Basin.||||||07-NOV-08
14553|Olney Formation|24551|5|Briefly described|p320, p731 Table 17.1|||Of the Renmark Group. Max thickness: 200m.||||||
14553|Olney Formation|30581|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
14553|Olney Formation|30934|6|Mentioned|Map legend|Eocene|Eocene|||||||
14553|Olney Formation|31741|6|Mentioned|p6|||||||||
14553|Olney Formation|31745|6|Mentioned|Map legend|Eocene|Eocene|||||||
14553|Olney Formation|31746|4|Described|p194|||||||||
14553|Olney Formation|32315|6|Mentioned|Fig. 2|||||||||
14553|Olney Formation|34757|6|Mentioned|p46|||||||||
14553|Olney Formation|34813|5|Briefly described|p63|||Mention on P62 also.||||||
14553|Olney Formation|35187|6|Mentioned|Table1|||||||||
14553|Olney Formation|37809|6|Mentioned|Fig.7|||||||||
14553|Olney Formation|37873|6|Mentioned|p1|||||||||
14553|Olney Formation|38293|4|Described|p22|||||||||
14553|Olney Formation|38601|6|Mentioned|p7|||||||||
14553|Olney Formation|39329|6|Mentioned|Fig.1|||||||||
14553|Olney Formation|39929|6|Mentioned|p269|||||||||
14553|Olney Formation|40520|6|Mentioned|Fig.5|||||||||
14553|Olney Formation|40820|6|Mentioned|Fig.4|||||||||
14553|Olney Formation|41136|5|Briefly described|p215|||||||||
14553|Olney Formation|41868|5|Briefly described|p551|||||||||
14553|Olney Formation|42125|5|Briefly described|p132|||||||||
14553|Olney Formation|42126|6|Mentioned|p149, p158|||||||||
14553|Olney Formation|42127|5|Briefly described|p219|||See also Fig.3||||||
14553|Olney Formation|42130|6|Mentioned|Fig.3 P265|||||||||
14553|Olney Formation|42133|6|Mentioned|p302|||||||||
14553|Olney Formation|42134|6|Mentioned|Fig.3 P335|||||||||
14553|Olney Formation|42137|6|Mentioned|p369|||||||||
14553|Olney Formation|42138|6|Mentioned|p388|||||||||
14553|Olney Formation|42184|6|Mentioned|p351|||||||||
14553|Olney Formation|42648|5|Briefly described|p45|||Renmark Group||||||
14553|Olney Formation|42813|6|Mentioned|p24|||||||||
14553|Olney Formation|42827|4|Described|p268|||see also Fig 8.3. Of Renmark Group.||||||25-MAR-08
14553|Olney Formation|42881|4|Described|Fig.3, P84|||||||||
14553|Olney Formation|42966|2|Defined|p100|Middle Miocene|Eocene|Of the Renmark Group.||||||13-OCT-08
14553|Olney Formation|43195|5|Briefly described|Map Legend|Early Oligocene|Middle Eocene|See also commentary on back of map. Of Renmark Group.||||||
14553|Olney Formation|43218|4|Described|Fig.3,p22||Tertiary|Of the Renmark Group.||||||25-MAR-08
14553|Olney Formation|43780|6|Mentioned|p6|||||||||
14553|Olney Formation|43791|6|Mentioned|p372, Fig1|||||||||
14553|Olney Formation|43804|6|Mentioned|Fig.2,p49|||||||||
14553|Olney Formation|43841|5|Briefly described|8||Tertiary|||||||
14553|Olney Formation|44133|5|Briefly described|p158, 152 Fig. 10.2|Middle Miocene|Middle Eocene|Of the Renmark Group. Geological Province: Murray Basin. Includes: Moorlands Lignite Member||||||
14553|Olney Formation|44188|5|Briefly described|Map Legend|Miocene|Eocene|Of the Renmark Group. Geological province: Murray Basin. Unconsolidated to poorly consolidated, thinly bedded, dark brown, grey, black, carbonaceous sand, silt, clay, brown coal, peat; commonly micaceous, pyritic, ferruginised.||||||15-MAY-08
14553|Olney Formation|44191|5|Briefly described|Map Legend||Middle Miocene|Informally subdivided into Lower, Middle and Upper Olney Formation.||||||
14553|Olney Formation|49038|4|Described|Table 2|||Briefly described p24.||||||25-MAR-08
14553|Olney Formation|49040|6|Mentioned|p10|||||||||
14553|Olney Formation|50154|5|Briefly described|p26, p132|||Of the Renmark Group. Overlies the Warina Sand. Geological Province: Murray Basin.||||||
14553|Olney Formation|60451|5|Briefly described|p95 Fig. 61.|||||||||
14553|Olney Formation|60452|4|Described|p33|Middle Eocene|Early Eocene|Formerly the 'upper' Renmark Beds (Harris, 1996). Now upgraded to formation status. Disconformably overlain by the Calivil Formation, unconformably overlain by Murray Group. Overlies: Warina Sand conformably. Age: 45Ma. Max. Thickness: 300m.||||||25-MAR-08
14553|Olney Formation|60461|5|Briefly described|Map legend|Eocene|Paleocene|Fluviolacustrine and paludal deposits: carbonaceous silt, clay, brown coal and ligneous sand; pyritic, unconsolidated to poorly consolidated.||||||
14553|Olney Formation|60491|4|Described|p15|Eocene|Eocene|Of the Renmark Group. Overlies the Warina Sand. Overlain by the Geera Clay. Geological Province: Murray Basin||||||
14553|Olney Formation|60538|5|Briefly described|p480 Fig. 19|||Geological Province: Murray Basin.||||||
14553|Olney Formation|60599|5|Briefly described|p15, p84|Early Pliocene|Middle Eocene|In the upper part of Renmark Group. Fine-grained marginal marine deposits. Geological Province: Murray Basin.||||||
14553|Olney Formation|61155|5|Briefly described|p3, p18|Middle Miocene|Middle Eocene|Of the Renmark Group.  Unconsolidated carbonaceous clastics - sands, silts, clays and peaty coals. Overlies Warina Sand. Overlain by and interfingers with Geera Clay. Thickness: 350m. Geological Province: Murray Basin.||||||
14553|Olney Formation|61185|5|Briefly described|p57, p15|Middle Miocene|Middle Eocene|In upper part of Renmark Group. Fine grained and relatively well-sorted distal deposits. Geological Province: Murray Basin.||||||03-JUL-13
14553|Olney Formation|61314|5|Briefly described|p129|Middle Miocene||Geological Province: Murray Basin.||||||
14553|Olney Formation|61837|5|Briefly described|p216|Middle Eocene|Middle Eocene|Carbonaceous silt, siltstone, sand and kaolinitic clay interbedded with lignite brown coal. Geological Province: Murray Basin.||||||
14553|Olney Formation|61964|3|Fully described|p14 Fig. 4, p139-141|Middle Miocene|Late Eocene|Of Renmark Group. Detailed lithology given. Commonly micaceous, pyritic or ferruginised horizons present. Unconformable below Calivil Formation. Thickness: 128m in type-section Victoria. Geological Province: Murray Basin. See also age discussion p.143||||||
14553|Olney Formation|62405|5|Briefly described|Map legend|Tertiary|Tertiary|Unconsolidated to poorly consol'd, thinly bedded, dark brown, grey, black carbonaceous sand, silt, clay, brown coal, peat; commonly micaceous, pyritic, ferruginised. Includes intercalations of poorly sorted, fine- to med.gr. quartz sand +polymictic sand.||||||
14553|Olney Formation|63887|5|Briefly described|p20, p21 Fig. 1|Early Oligocene|Paleocene|Of Renmark Group. Floodplain and swamp environments dominates, resulting in deposition of carbonaceous sand, clay and silt.||||||
14553|Olney Formation|65552|5|Briefly described|p5 Fig. 3, p6|Middle Miocene|Early Eocene|Of Renmark Group. Predominantly fluvial and lacustrine unit deposited contemporaneously with the marine Murray Group, Winnambool and Ettrick formations and Geera Clay. Underlies Wunghnu Group units, unconformably overlies Warina Sand.||||||
14553|Olney Formation|65969|5|Briefly described|p27 Tb.3.3, p30-1|Early Oligocene|Eocene|Of Renmark Group. Fluvial to paralic carbonaceous silt and clay; minor lignite: four resources identified by CRA Exploration but had excess ash, sulfur and overburden. Unconformable on Paleozoic basement. Upper contact is erosional with Calivil Formation. Over 100 m thick in the north of the BENDIGO 1:250 000 sheet. No magnetic response.||||||
14553|Olney Formation|66012|5|Briefly described|p17|||In Murray Basin. Of Renmark Group. Probable correlative of Dilwyn Formation|| ||||13-JUN-13
14553|Olney Formation|66286|5|Briefly described|p179.|||||Unit in Renmark Group.||Overlies Warina Sand.|Interbedded fluvio-lacustrine sands, silts and clays.|
14553|Olney Formation|67462|5|Briefly described|Map legend.|Early Miocene|Late Eocene|Murray Basin.||||||
14553|Olney Formation|68189|5|Briefly described|p3, p26, p27 Tb.3.2, p33|Miocene|Eocene|The oldest unit recorded in ST ARNAUD.  Middle Eocene to Lower Miocene age. Time equivalent of the upstream White Hills Granite in ST ARNAUD. Fluvial to paludal depositional environment.||Of the Renmark Group.||Disconformably overlain by the Parilla Sand. Overlain by the Geera Clay. Overlain by the Winnambool Formation.|Comprises carbonaceous sand, silt and clay, lignite.|
14553|Olney Formation|68194|5|Briefly described|p23|||||Unit in Renmark Group.||Overlies Warina Sand.|Carbonaceous siltstone and claystone.|
14553|Olney Formation|68715|6|Mentioned|p31 Fig.5|Chattian|Bartonian|Murray Basin.||Renmark Group.||||07-APR-17
14553|Olney Formation|69163|5|Briefly described|Map legend|Tertiary|Tertiary|Murray Basin.|||||Unconsolidated to poorly consolidated, thinly-bedded, dark brown, grey, black, carbonaceous sand, silt, clay, brown coal, peat; commonly micaceous, pyritic, ferruginised; intercalated poorly-sorted fine-medium quartz sand and polymictic sand.|
14553|Olney Formation|69798|5|Briefly described|p4 Fig.2, p11|Miocene|Eocene|Murray Basin. Appears as Onley Formation in Fig.2. Seismic profiles.||Renmark Group.||||
14553|Olney Formation|70718|5|Briefly described|p17, p24-p25, p103|Middle Miocene|Early Eocene|Murray Basin. Previously the Upper Renmark Beds. Is one of the primary aquifers in the Hay map sheet area. Informally subdivided into an upper, middle and lower units. Up to 300m thick. Hosts more lignitic coal than any other formation in the Murray Basin. Deposition was intermittent in the eastern part of the Murray Basin. A second lithology description is provided in the appendix, p103.||Renmark Group|||Terrigenous clastic sands and clays with common interbeds of lignitic brown coal and peat.|
14553|Olney Formation|71593|5|Briefly described|p52-p54|Miocene|Oligocene|||Renmark Group||||
14553|Olney Formation|72445|5|Briefly described|App1; App.2; App.7 p2, p4-5, p7-8, p10|Miocene|Eocene|See also p13-14, p16-21. Data indicates deposition over weathered Palaeozoic bedrock during the Late Eocene but the precise timing needs to be confirmed. Shown on the 'Lithostratigraphy of Cenozoic sediments in the Murray Basin' (from Brown & Stephenson 1991). App.2 is a .csv format file. Identified in Stavely 04, 05,11,14,16. Pollen/spores identified in samples from Stavely 04, 11, 14. Dominantly micaceous and lignitic sand. Locally silty, muddy and gravelly. Sparse <1m intervals of lignite. Said to be non-marine, alluvial fan, fluvial.||Renmark Group||Underlies Calivil Formation, sharp contact; Ettrick Formation, gradational/sharp contact; Buccleuch beds. Partially equivalent to Murray Group. Overlies Glenthompson Sandstone, gradational.|Shown as including lignites and thick fluvio-lacustrine sands, silts and clays and mud beds in a fine sand.|
14553|Olney Formation|73118|5|Briefly described|p12, 17-18, 21, 24, 30, 34, 45, 48, 53|Miocene|Eocene|See also p64, 80, 83. Murray Basin. Has potential as a source of groundwater. Drill core summary logs. 200m thick. Entirely concealed, yet forms a thin, virtually continuous blanket beneath almost the entire Basin. Includes 'Upper Renmark beds' in SA. Fluvio-lacustrine, meandering channel, flood-plain, and swamp environments; includes deltaic and paralic sediments towards top.||Renmark Group.||Overlies Warina Sand, Glenthompson Sandstone and Saint Arnaud Group. Is overlain by Ettrick Formation, Geera Clay, Winnambool Formation and Loxton-Parilla Sands.|Un- to poorly-consolidated, thinly bedded dark carbonaceous silt, sand, clay, brown coal, peat; commonly micaceous, pyritic, ferruginised. Sand, sandy dolomite intercalations. Contains large uneconomic deposits of brown coal.|
14553|Olney Formation|73188|6|Mentioned|p320|Oligocene|Oligocene|Murray Basin.|||||Limestone, marl, clay.|
14553|Olney Formation|73228|4|Described|p50, p53-57, p60|Middle Miocene|Late Paleocene|Murray Basin. Floodplain and swamp sediments also with fluvial, lacustrine, and marginal marine (upper portion) depositional settings. Inferred to be mainly deposited in the vicinity of a coastal swamp based also on fossil content. Identified in Nadda 1 drillhole. More widespread than the underlying Warina Sand. [Also consists of a younger phase assigned to the Murray Group? See p55].||Renmark Group|Moorlands Lignite Member|Underlain by Warina Sand. Overlain by Ettrick Formation.|Alternating multi-coloured sandy silt and silty clay, thinly bedded grey to green carbonaceous sand, silt, clay and lignite.|
14553|Olney Formation|73229|6|Mentioned|p67|Early Miocene|Late Early Oligocene|Murray Basin.||Renmark Group||||31-OCT-22
14553|Olney Formation|73505|4|Described|p2, p10-11, p13-14, p36|Oligocene|Eocene|Murray Basin. Contains abundant plant material. Unconformable on Paleozoic basement, upper erosional contact. Topped by the Mologa Surface, Norval Regolith. No detectable magnetic response.||Renmark Group||Overlies Warina Formation, underlies Murray Group and Norval Regolith, underlies Calivil Formation with erosional contacts|Carbonaceous fluvial to lacustrine and paralic siltstone to claystone, contains brown coal with high levels of sulphur and ash. Thickness of 100+/-25 m.|
14592|Oodnadatta Formation|12597|5|Briefly described|p492 Tb.1, p500|Albian|Albian|SW Eromanga Basin. Up to 300m thick.|||||Calcareous mudstone and siltstone with minor thin interbeds of fine-grained calcareous sandstone. Contains a rich marine fauna of bivalves, ammonites and gastropods.|
14592|Oodnadatta Formation|13497|5|Briefly described|p115 fig 6.33, p152-p154, |Early Cretaceous|Early Cretaceous|Eromanga Basin.||Marree Subgroup||Overlies the Coorikiana Sandstone. Overlain by the Mackunda Formation and the Winton Formation.||
14592|Oodnadatta Formation|13516|5|Briefly described|p167 fig 10, p171 fig 12|Albian|Albian|In Eromanga Basin.||Of Marree Subgroup||||
14592|Oodnadatta Formation|22883|5|Briefly described|Fig2 P30||Early Cretaceous|Overlying unit is Mackunda Formtion, underlying unit is Coorikiana Sandstone||||||
14592|Oodnadatta Formation|22912|5|Briefly described|33|||Geol province Eromanga Basin||||||
14592|Oodnadatta Formation|23054|5|Briefly described|p21,26-7|Albian|Albian|||||||
14592|Oodnadatta Formation|23056|6|Mentioned|12 table 2|||||||||
14592|Oodnadatta Formation|23154|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|Geological Province - Eromanga Basin.  Parent - Marree Subgroup of the Neales River Group.||||||
14592|Oodnadatta Formation|23155|4|Described|p31|Early Cretaceous|Early Cretaceous|The Oodnadatta Formation is of Early Cretaceous (Albian) age, based on spore pollen assemblages.||||||
14592|Oodnadatta Formation|23375|4|Described|Fig2 p265||Albian|Laterally equivalent to Toolebuc Formation and Allaru Mudstone. Of Eromanga Basin.||||||16-SEP-08
14592|Oodnadatta Formation|23818|5|Briefly described|p141 Fig.65, p144 Fig.66, p158|Cretaceous|Cretaceous|Geological Province: Great Artesian Basin. Of the Neales River Group. Max. thickness: ~2000 ft.||||||
14592|Oodnadatta Formation|23830|5|Briefly described|Fig. 3a|Cretaceous|Cretaceous|Geological Province: Boorthanna Trough, eastern Arckaringa Basin.||||||
14592|Oodnadatta Formation|23982|5|Briefly described|p58 Fig.18|||Of Neales River Group. Geological Province: Eromanga Basin.||||||
14592|Oodnadatta Formation|24092|5|Briefly described|p8 Fig.3|||Of Neales River Group. Geological Province: Eromanga Basin.||||||
14592|Oodnadatta Formation|24175|3|Fully described|p27, p17 Fig. 3|Albian|Albian|Of Marree Subgroup.  Overlies Coorikiana Sandstone.  Max. thickness: 229m.  Geological Province: Eromanga Basin.||||||
14592|Oodnadatta Formation|24210|5|Briefly described|p133 Fig. 2|Late Cretaceous|Early Cretaceous|Of the Marree Subgroup.  Geological Province: Eromanga Basin.||||||
14592|Oodnadatta Formation|24321|5|Briefly described|Map legend|Albian|Albian|Parent: Marree Subgroup||||||
14592|Oodnadatta Formation|29379|6|Mentioned|p25|||Tambo Formation equivalent.||||||
14592|Oodnadatta Formation|29651|6|Mentioned|p25|||||||||
14592|Oodnadatta Formation|29660|6|Mentioned|Fig.1|||||||||
14592|Oodnadatta Formation|30539|6|Mentioned|p6|||Angiosperms||||||
14592|Oodnadatta Formation|30540|6|Mentioned|Fig.6|||||||||
14592|Oodnadatta Formation|30803|6|Mentioned|p1|||Cretaceous||||||
14592|Oodnadatta Formation|30804|6|Mentioned|p7|||See also P10, Table 1||||||
14592|Oodnadatta Formation|30807|6|Mentioned|p102|||Suggested map symbol||||||
14592|Oodnadatta Formation|30919|6|Mentioned|Map legend|Albian|Albian|||||||
14592|Oodnadatta Formation|30921|6|Mentioned|Map legend|Turonian|Albian|Neocomian - Turonian ?||||||
14592|Oodnadatta Formation|30924|6|Mentioned|Map legend|Albian|Albian|||||||
14592|Oodnadatta Formation|31208|6|Mentioned|Fig. 7|||||||||
14592|Oodnadatta Formation|31249|6|Mentioned|p63|||||||||
14592|Oodnadatta Formation|31699|4|Described|p133|||L.Cretaceous||||||
14592|Oodnadatta Formation|31923|6|Mentioned|p14|||||||||
14592|Oodnadatta Formation|32314|6|Mentioned|Fig. 4|||||||||
14592|Oodnadatta Formation|33075|6|Mentioned|Table 1|||Refers Wopfner et al. (1970)||||||
14592|Oodnadatta Formation|33490|6|Mentioned|p30|||Cret. Correlation||||||
14592|Oodnadatta Formation|33491|4|Described|p56|||Mention Fig.2||||||
14592|Oodnadatta Formation|33521|6|Mentioned|p8|||L. Cret.||||||
14592|Oodnadatta Formation|33819|6|Mentioned|p3|||||||||
14592|Oodnadatta Formation|33820|6|Mentioned|Map legend|Albian|Neocomian|Neocomian - Albian||||||
14592|Oodnadatta Formation|33821|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
14592|Oodnadatta Formation|33822|6|Mentioned|Map legend|Albian|Neocomian|Neocomian - Albian||||||
14592|Oodnadatta Formation|33823|6|Mentioned|Map legend|Cenomanian|Neocomian|Neocomian - Cenomanian||||||
14592|Oodnadatta Formation|33824|6|Mentioned|p12|||See also Table 2||||||
14592|Oodnadatta Formation|33825|5|Briefly described|p8|||Lithology||||||
14592|Oodnadatta Formation|33827|6|Mentioned|p13|||See also Table 2||||||
14592|Oodnadatta Formation|33828|6|Mentioned|p9|||See also Table 1||||||
14592|Oodnadatta Formation|33831|6|Mentioned|Map legend|Cenomanian|Neocomian|Neocomian - Cenomanian||||||
14592|Oodnadatta Formation|33832|6|Mentioned|p6|||Stratigraphy||||||
14592|Oodnadatta Formation|33936|6|Mentioned|Fig.3A|||Cretaceous.||||||
14592|Oodnadatta Formation|33938|6|Mentioned|p41|||O'lain by Eyre Fm.||||||
14592|Oodnadatta Formation|33939|5|Briefly described|p386|||See also P405. L.Cret.||||||
14592|Oodnadatta Formation|33971|5|Briefly described|p37|||See also Fig.15.||||||
14592|Oodnadatta Formation|34611|6|Mentioned|Fig.65|||Cretaceous. See also Fig.66||||||
14592|Oodnadatta Formation|34725|6|Mentioned|p379|||||||||
14592|Oodnadatta Formation|34984|6|Mentioned|p323|||||||||
14592|Oodnadatta Formation|36490|6|Mentioned|p173|||||||||
14592|Oodnadatta Formation|36494|6|Mentioned|p145|||||||||
14592|Oodnadatta Formation|36552|6|Mentioned|p62|||||||||
14592|Oodnadatta Formation|36571|6|Mentioned|p101|||See also Table 4.||||||
14592|Oodnadatta Formation|36733|6|Mentioned|p14|||||||||
14592|Oodnadatta Formation|36922|6|Mentioned|Fig.3|||||||||
14592|Oodnadatta Formation|37776|6|Mentioned|Fig.2|||||||||
14592|Oodnadatta Formation|38007|6|Mentioned|p38|||||||||
14592|Oodnadatta Formation|38022|6|Mentioned|p29|||||||||
14592|Oodnadatta Formation|38068|5|Briefly described|p72|||||||||
14592|Oodnadatta Formation|38199|6|Mentioned|p426|||||||||
14592|Oodnadatta Formation|38814|6|Mentioned|Table 1|||||||||
14592|Oodnadatta Formation|39211|5|Briefly described|Fig.6|||See also Figs 9-16 etc||||||
14592|Oodnadatta Formation|39352|6|Mentioned|Map legend|Albian|Aptian|Aptian to Albian||||||
14592|Oodnadatta Formation|39914|6|Mentioned|p2|||||||||
14592|Oodnadatta Formation|40003|6|Mentioned|Fig.9|||See also Table 7.||||||
14592|Oodnadatta Formation|40058|6|Mentioned|p5|||||||||
14592|Oodnadatta Formation|40199|6|Mentioned|p16|||||||||
14592|Oodnadatta Formation|40220|6|Mentioned|Fig.2|||||||||
14592|Oodnadatta Formation|40670|6|Mentioned|Fig.9|||||||||
14592|Oodnadatta Formation|40681|6|Mentioned|Fig.2|||||||||
14592|Oodnadatta Formation|40801|6|Mentioned|p85|||||||||
14592|Oodnadatta Formation|40910|6|Mentioned|p15|||||||||
14592|Oodnadatta Formation|40911|6|Mentioned|Map legend|Cenomanian|Cenomanian|Prob. Cenomanian||||||
14592|Oodnadatta Formation|40925|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
14592|Oodnadatta Formation|40926|3|Fully described|p17|||||||||
14592|Oodnadatta Formation|41012|6|Mentioned|p143|||||||||
14592|Oodnadatta Formation|41060|6|Mentioned|Fig.3|||||||||
14592|Oodnadatta Formation|41062|6|Mentioned|Fig.5|||||||||
14592|Oodnadatta Formation|41064|6|Mentioned|p62|||||||||
14592|Oodnadatta Formation|41084|5|Briefly described|Fig.2|||||||||
14592|Oodnadatta Formation|41085|3|Fully described|p88|||||||||
14592|Oodnadatta Formation|41086|3|Fully described|p98|||||||||
14592|Oodnadatta Formation|41087|3|Fully described|p123|||||||||
14592|Oodnadatta Formation|41088|6|Mentioned|p141|||||||||
14592|Oodnadatta Formation|41098|4|Described|p176|||||||||
14592|Oodnadatta Formation|41117|6|Mentioned|Fig.2|||||||||
14592|Oodnadatta Formation|41165|5|Briefly described|p362|||See also Fig.15||||||
14592|Oodnadatta Formation|41175|6|Mentioned|Fig.1|||||||||
14592|Oodnadatta Formation|41177|6|Mentioned|Fig.2|||||||||
14592|Oodnadatta Formation|41182|5|Briefly described|Fig.2|||||||||
14592|Oodnadatta Formation|41183|6|Mentioned|Fig.3 p308|||||||||
14592|Oodnadatta Formation|41187|6|Mentioned|Fig.2|||||||||
14592|Oodnadatta Formation|41216|6|Mentioned|Fig.18|||||||||
14592|Oodnadatta Formation|41266|6|Mentioned|Fig.3|||||||||
14592|Oodnadatta Formation|41523|3|Fully described|p276|||||||||
14592|Oodnadatta Formation|41533|6|Mentioned|p263|||||||||
14592|Oodnadatta Formation|41950|5|Briefly described|Fig.2 P3|||||||||
14592|Oodnadatta Formation|42003|6|Mentioned|p141|||||||||
14592|Oodnadatta Formation|42071|6|Mentioned|Fig.2A P116|||||||||
14592|Oodnadatta Formation|42293|6|Mentioned|Fig.2 P.18|||||||||
14592|Oodnadatta Formation|42375|6|Mentioned|Fig.28 P125, Table 1|Late Cretaceous|Jurassic|Eromanga Basin||||||
14592|Oodnadatta Formation|42395|5|Briefly described|Fig.13 P83|||||||||
14592|Oodnadatta Formation|42520|6|Mentioned|p6|||Old/alternate name for the Cadna-owie Formation?||||||
14592|Oodnadatta Formation|42746|4|Described|p12|||||||||
14592|Oodnadatta Formation|42905|5|Briefly described|p20|||of Marree Subgroup||||||
14592|Oodnadatta Formation|43053|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Marine mudstone.||||||25-MAY-05
14592|Oodnadatta Formation|43258|5|Briefly described|Map Legend||Cretaceous|||||||
14592|Oodnadatta Formation|43298|5|Briefly described|Map Legend||Cretaceous|||||||
14592|Oodnadatta Formation|43591|6|Mentioned|p40,165|||||||||
14592|Oodnadatta Formation|43628|6|Mentioned|Fig.3|Early Cretaceous|Early Cretaceous|||||||
14592|Oodnadatta Formation|43681|5|Briefly described|p296|||||||||
14592|Oodnadatta Formation|44133|4|Described|p122, 104 Fig. 9.11|Late Albian|Middle Albian|Geological Province: Eromanga Basin. Includes: Woolridge Limestone Member. Previously included Coorikiana Sandstone and Mount Alexander Sandstone, now separate formations. Thickness: ~300m. Conformably underlies Mackunda Formation.||||||
14592|Oodnadatta Formation|44289|5|Briefly described|Map Legend||Albian|||||||
14592|Oodnadatta Formation|44658|14|Not recorded|map legend|||Neocom-Ablian. (G53-15).||||||
14592|Oodnadatta Formation|45132|6|Mentioned|p15|||||||||
14592|Oodnadatta Formation|46791|6|Mentioned|Table 2|||||||||
14592|Oodnadatta Formation|46937|5|Briefly described|Fig.10|||See also Table 1.||||||
14592|Oodnadatta Formation|49010|6|Mentioned|Fig.4|||Eromanga Basin||||||
14592|Oodnadatta Formation|49011|6|Mentioned|Fig.3|||Eromanga Basin||||||
14592|Oodnadatta Formation|60717|5|Briefly described|p40 Fig. 2|Early Cretaceous|Early Cretaceous|Overlies Coorikiana Sandstone; interfingers laterally with Mackunda Formation. Overlain by Winton Formation. Geological Province: Eromanga  Basin.||||||31-JAN-08
14592|Oodnadatta Formation|60953|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Marine mudstone.||||||
14592|Oodnadatta Formation|61014|6|Mentioned|p533 Fig.2.|Early Cretaceous|Early Cretaceous|Eromanga Basin.||||Overlies Coorikiana Sandstone.||21-JAN-15
14592|Oodnadatta Formation|61108|5|Briefly described|map legend|Cretaceous|Cretaceous|Marine mudstone.||||||01-JUN-05
14592|Oodnadatta Formation|61613|6|Mentioned|p282 Fig. 2|Early Cretaceous|Early Cretaceous|Of Maree Subgroup. Geological Province: Eromanga Basin.||||||07-FEB-11
14592|Oodnadatta Formation|61615|6|Mentioned|p302 Fig. 2|Late Cretaceous|Early Cretaceous|Geological Province: Eromanga Basin.||||||07-FEB-11
14592|Oodnadatta Formation|62029|5|Briefly described|p15 Fig. 4|Cretaceous|Cretaceous|||||||
14592|Oodnadatta Formation|62537|6|Mentioned|p191 Fig.2. |Late Cretaceous|Early Cretaceous|Eromanga Basin.||||Overlies Coorikiana Formation and Bulldog Shale. Is overlain by Mackunda Formation.||
14592|Oodnadatta Formation|62730|5|Briefly described|p352 Fig. 1|Cretaceous|Cretaceous|Geological Province: Eromanga Basin.||||||21-APR-08
14592|Oodnadatta Formation|63979|5|Briefly described|Fig. 44|Cenomanian|Albian|Overlies Coorikiana Sandstone. Underlies Mackunda Formation.||||||07-FEB-11
14592|Oodnadatta Formation|64197|6|Mentioned|p625 Fig.1c, p630 Fig.6|Cretaceous|Cretaceous|Eromanga Basin.||Unit in Marree Subgroup.||Overlies Coorikiana Sandstone; underlies Winton or Mackunda Formations.||
14592|Oodnadatta Formation|65385|5|Briefly described|pS134 Fig.7|Early Cretaceous|Early Cretaceous|Of Eromanga Basin. Overlies Coorikiana Sandstone. Overlain by Mackunda Formation.||||||08-MAR-12
14592|Oodnadatta Formation|65489|5|Briefly described|p96, p155|Early Cretaceous|Early Cretaceous|Eromanga Basin. 300m thick. Appears as Oodnadatta Sandstone on p96.||||Overlies Coorikiana Sandstone and Bulldog Shale.||
14592|Oodnadatta Formation|65925|5|Briefly described|Appendix 2.||||||||Interbedded claystone and siltstone, with fine-grained sandstone, calcareous and ferruginous concretions; limestone with celestite and baryte veins.|
14592|Oodnadatta Formation|66518|5|Briefly described|p19.|Cretaceous|Cretaceous|Eromanga Basin.||Unit in Marree Subgroup.||Overlies Bulldog Shale and, locally, Coorikiana Sandstone. Is overlain by Mackunda Formation.||
14592|Oodnadatta Formation|66529|6|Mentioned|p12 Fig.5|||||Unit in Neales River Group.|Includes Wooldridge Limestone Member.|||
14592|Oodnadatta Formation|66623|6|Mentioned|p265.|||Equivalent in part to Allaru Mudstone, Koonenberry Belt.||||||
14592|Oodnadatta Formation|67120|5|Briefly described|Map legend|Cretaceous|Cretaceous||||||Claystone and siltstone, interbedded; with fine-grained sandstone, calcareous and ferruginous concretions; limestone with celestite and barite veins.|
14592|Oodnadatta Formation|67462|5|Briefly described|Map legend.|Late Cretaceous|Early Cretaceous|Eromanga Basin.||||Overlies Coorikiana Formation and Bulldog Shale. Is overlain by Winton Formation.||
14592|Oodnadatta Formation|67578|6|Mentioned|p335 Fig.2|Cretaceous|Cretaceous|Lake Eyre region.||||||
14592|Oodnadatta Formation|67784|6|Mentioned|p26, p28 table 1|||Southern Eromanga Basin. Correlations based on belemnites.||||Overlies Coorikiana Sandstone. Correlated with Allaru Formation, Toolebuc Formation.||08-FEB-18
14592|Oodnadatta Formation|68068|5|Briefly described|Map legend|Albian|Albian|Eromanga Basin. Recognised in subsurface; surface exposures often indistinguishable from Bulldog Shale if no Coorikiana Sandstone present. Shallow marine.||Unit in Marree Subgroup.||Conformably overlies Coorikiana Sandstone. Is overlain conformably by Mackunda Formation.|Dark grey to grey mudstone with fossiliferous limestone concretions (molluscs, forams, wood, microflora, fish, vertebrates); bioturbated, interbedded with calcareous siltstone and fine-grained sandstone.|
14592|Oodnadatta Formation|68206|6|Mentioned|p31-33|Albian|Albian|S Eromanga Basin.||||A partial correlative of Allaru and Toolebuc Formations.||
14592|Oodnadatta Formation|68713|5|Briefly described|p22|Cretaceous|Cretaceous|||Of the Marree Subgroup.||||
14592|Oodnadatta Formation|68715|6|Mentioned|p30 Fig.5|Albian|Albian|Eromanga Basin.||||||
14592|Oodnadatta Formation|68734|5|Briefly described|p218 Fig.2, p221 Fig.3|Albian|Albian|Eromanga Basin (SW). Shallow marine.||Of the Rolling Downs Group.||||18-NOV-14
14592|Oodnadatta Formation|69019|4|Described|p83 Fig.20, p85 Fig.21, p98-99.|Albian|Albian|SW Eromanga Basin. Defined by Freytag et al. (1967). Type section at Mt Arthur, ~55 km E of Oodnadatta. It is almost impossible to distinguish this unit in the field from Bulldog Shale where Coorikiana Sandstone is absent; the general term Marree Subgroup is used on the map where this is the case. Thickness from ~40 m to 344.6 m max.||Unit in Marree Subgroup.||Overlies Coorikiana Sandstone conformably. Is overlain conformably by Mackunda Formation.|Grey laminated siltstone or mudstone with grey calcareous concretions, under dark grey mudstone and siltstone with fine-grained glauconitic and feldspathic sandstone interbeds. Slightly carbonaceous and finely micaceous; conspicuous shell fragments.|
14592|Oodnadatta Formation|69023|5|Briefly described|p87, p89 Fig.20, p93, p99-100, p102-103|Albian|Albian|See also p105, p191-192. Defined by Freytag et al.(1967). Where Coorikiana Sandstone is absent, the in-field recognition of Oodnadatta Formation is difficult: the name Marree Subgroup is applied. Thickness from <20 to >180m. Lithologically similar to Allaru Mudstone. Trace fossil assemblages similar to those in Bulldog Shale. Stratigraphic wells intersection data.||Unit in Marree Subgroup.||Conformably overlies Coorikiana Sandstone. Equivalent to Allaru Mudstone. Is overlain conformably by Mackunda Formation.|A lower unit of siltstone with calcareous concretions is overlain by dark grey mudstone and siltstone with fine-grained glauconitic and feldspathic sandstone interbeds; zones of bioturbation.|
14592|Oodnadatta Formation|69457|5|Briefly described|p41:3, 6-8, 11-12, 17|Early Cretaceous|Early Cretaceous|Freytag (1966). SW Eromanga Basin. The lower part of this unit, together with Bulldog Shale and Coorikiana Sandstone, is equivalent to the Wallumbilla Formation. The middle and upper part of this unit is equivalent to the combined Toolebuc Formation and Allaru Mudstone.||Marree Subgroup.||Overlies Coorikiana Sandstone. Is overlain conformably by Mackunda Formation. Correlative of Allaru Mudstone.|Claystone and siltstone with interbeds of fine-grained sandstone, calcareous and ferruginous concretions, and cone-in-cone limestone. Contains a rich fossil assemblage.|12-JUL-16
14592|Oodnadatta Formation|69562|6|Mentioned|p681-682|Mesozoic|Mesozoic|A relatively conductive sandy unit.||Unit in Marree Subgroup.||||
14592|Oodnadatta Formation|69594|6|Mentioned|p530|||||||Is correlated with the Allaru Mudstone.||
14592|Oodnadatta Formation|69673|6|Mentioned|p155 fig 127|Cretaceous|Cretaceous|||||Overlies Coorikiana Sandstone, overlain by Mackunda Formation||
14592|Oodnadatta Formation|69797|5|Briefly described|p17 Fig.2|Early Cretaceous|Early Cretaceous|Geol. Prov: Eromanga Basin.||||||
14592|Oodnadatta Formation|69946|3|Fully described|p22-24, p57, p94, p120-122|Early Cretaceous|Early Cretaceous|Freytag (1966). Type section is Mount Arthur, E of Oodnadatta. Up to c.300m thick. Contains a varied marine fauna. Middle-late Albian. Wireline log correlations.||Unit in Marree Subgroup.||Conformably overlies Coorikiana Sandstone. Is overlain conformably by Mackunda Formation. Passes laterally into Wallumbilla and Toolebuc Formations, Allaru Mudstone and Marree Subgroup.|Laminated and thin-bedded claystone and siltstone with interbeds of fine-grained sandstone; calcareous and ferruginous concretions and a thin unit of calcareous siltstone and fossil-rich concretionary limestone in the lower part of the unit.|
14592|Oodnadatta Formation|69947|5|Briefly described|p13 Fig.7.2|Late Cretaceous|Early Cretaceous|Eromanga Basin.||Marree Subgroup.||||
14592|Oodnadatta Formation|69948|6|Mentioned|Figs.4.1, 18|||Eromanga Basin.||||Overlies Bulldog Shale.||
14592|Oodnadatta Formation|70336|5|Briefly described|Map legend|Cretaceous|Cretaceous|||Of Marree Subgroup.|||Interbedded claystone and siltstone, with fine-grained sandstone, calcareous and ferruginous concretions; limestone with celestite and barite veins.|12-JAN-16
14592|Oodnadatta Formation|70383|5|Briefly described|p45|Albian|Albian|Eromanga Basin. Marine deposits.||||||
14592|Oodnadatta Formation|70789|5|Briefly described|p318, p320 Fig.4|Cenomanian|Cenomanian|Eromanga Basin.|c.93 Ma.||||Marine mudstones, siltstones and shales.|
14592|Oodnadatta Formation|70821|5|Briefly described|p21 Fig.2.6, p23|Early Cretaceous|Early Cretaceous|Eromanga Basin.||||Overlies Coorikiana Sandstone. Is overlain by Toolebuc Formation.||
14592|Oodnadatta Formation|70823|5|Briefly described|p43-p44|Early Cretaceous|Early Cretaceous|Eromanga Basin. Up to 300m thick. Deposited in a restricted, stratified and anoxic marine environment.||||Overlies the Coorikiana Sandstone. Overlain by the Mackunda and Winton Formations.||
14592|Oodnadatta Formation|70860|6|Mentioned|p281|||Great Artesian Basin.||||||
14592|Oodnadatta Formation|70938|5|Briefly described|p807-808|Early Cretaceous|Early Cretaceous|||Neales River Group.||||
14592|Oodnadatta Formation|71321|5|Briefly described|p15,65|Cenomanian|Cenomanian|Of Eromanga Basin. Regressivee depositional package following peak early Cretaceous marine transgression; shallow marine-fine-graned siliciclastics.||||Overlies the Bulldog Shale.||24-OCT-19
14592|Oodnadatta Formation|71342|3|Fully described|Ch1 p19, Ch4 p8, Ch5 p23-p24|Albian|Albian|Defined by Freytag (1966) as the fossiliferous siltstone and shale overlying the Bulldog Shale. Freytag also assigned the type section at Mount Arthur east of Oodnadatta. A maximum thickness of up to 300m is recorded in the Moomba area. Age derived from palynology studies and from macrofossil assemblage. Interpreted to have been deposited in a low-energy, shallow marine environment. Spore-pollen zone is given in Ch5 p57. Forms a seal over the Coorikiana Sandstone.  Laterally equivalent to the Wallumbilla Formation, Toolebuc Formation and Allaru Mudstone. See also  Ch5 p27, Ch5 p33, Ch5 p57, Ch5 p122-p124, Ch6 p10, Ch7 p13, Ch9 p21, Ch11 p5.||Marree Subgroup||Conformably overlies the Coorikiana Sandstone. Overlies the Bulldog Shale. Conformably overlain by the Mackunda Formation. Overlain by the Winton Formation.|Laminated and thinly-bedded claystone and siltstone with interbeds of fine-grained sandstone, calcareous siltstone and fossil-rich concretionary limestone.|
14592|Oodnadatta Formation|71348|6|Mentioned|p202|||Geological province: Gawler Craton.||||||
14592|Oodnadatta Formation|72298|5|Briefly described|p801|Cretaceous|Cretaceous|Eromanga Basin (SA).||Neales River Group.|Wooldridge Limestone Member.|Overlies Coorikiana Sandstone. Is overlain by Mackunda FZ.||
14592|Oodnadatta Formation|72456|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Marree 1:250k map sheet.|||||Claystone and siltstone, interbedded with fine-grained sandstone, calcareous and ferruginous concretions; limestone with celestite and barite veins,|
14592|Oodnadatta Formation|72476|6|Mentioned|p36 Fig.9|||Eromanga Basin. Time-temperature thermal history diagram.||||||
14592|Oodnadatta Formation|73167|6|Mentioned|p664 Fig. 2|Cretaceous|Cretaceous|Eromanga Basin.||||||
14592|Oodnadatta Formation|73249|4|Described|p316-319, p320 Fig.2, p321-338|Albian|Albian|Eromanga Basin. Maximum age of mid-Albian, minimum age of late Albian. Up to 300m thick. Lateral variations in mineralogy between drill holes, dominant clay mineral is montmorillonite. Deposited in a shallow marine environment, more arid and warmer environment than the Cadna-owie Formation. Sediment sources interpreted to be a mix of felsic to mafic igneous rocks from the west and south.||||Conformably overlies the Coorikiana Sandstone, lateral equivalent of the Allaru Mudstone.|Laminated and thin-bedded claystone and siltstone, up to 300m thick.|
14592|Oodnadatta Formation|73251|6|Mentioned|p36, p62|Early Cretaceous|Early Cretaceous|Eromanga Basin, Frome Embayment. Marginal thermal maturity.||||Underlain by Bulldog Shale and Coorikiana Sandstone. Overlain by and equivalent to Mackunda Formation. Equivalent to Allura Mudstone and Toolebuc Formation.||
14592|Oodnadatta Formation|73281|6|Mentioned|Appendix (DIP)|||See DIP034_Petroleumdata.xlsx and DIP034_Welldata.xlsx.||||||
14592|Oodnadatta Formation|73343|6|Mentioned|p337|Cretaceous|Cretaceous|Eromanga Basin.||||Underlain by Coorikiana Sandstone. Overlain by Winton Formation. Equivalent to Allaru Mudstone and Toolebuc Formation.||
14592|Oodnadatta Formation|73479|5|Briefly described|p156 Fig.2, p159|Cretaceous|Cretaceous|Eromanga Basin. Open shallow marine depositional environment.|ca 104-98 Ma|||Overlies Coorikiana Sandstone, underlies Winton Formation||
14596|Ooldea Sand|22587|6|Mentioned|p79 Fig.7|Late Eocene|Late Eocene|||||||
14596|Ooldea Sand|22613|4|Described|p21|Early Oligocene|Late Eocene|||||||
14596|Ooldea Sand|22614|5|Briefly described|map|Eocene|Eocene|||||||
14596|Ooldea Sand|23488|6|Mentioned|p38 Fig. 5, p41|||See also p39 Fig. 5.  Geological Province: Eucla Basin.||||||
14596|Ooldea Sand|24396|6|Mentioned|p218 Fig.3, p223|||Referred to as Upper and Lower Ooldea and "Upper" and "Lower" Ooldea Sand in this article. Geological Province: Gawler Craton.||||||
14596|Ooldea Sand|24397|4|Described|p240|||Can be subdivided into informal units; "upper" Ooldea Sand and "lower" Ooldea Sand.  Geological Province: Eucla Basin.||||||
14596|Ooldea Sand|24606|5|Briefly described|p956, p958 Fig. 3|Late Eocene|Late Eocene|Geological Province: Eucla Basin||||||
14596|Ooldea Sand|24617|6|Mentioned|p114, p115 Fig. 3, p125 Fig. 10|Eocene|Eocene|Geological Province: Eucla Basin.||||||15-APR-09
14596|Ooldea Sand|42086|5|Briefly described|Fig.2 P4|||Reserved as Ooldea||||||
14596|Ooldea Sand|42356|5|Briefly described|Fiche 7 P15 Table 2|late Eocene||See also Microfiche 7 Fig.4||||||
14596|Ooldea Sand|42816|4|Described|p23|||||||||
14596|Ooldea Sand|44133|5|Briefly described|p182, 180 Fig. 10.22|Miocene|Miocene|Geological Province: Eucla Basin. Thickness: 112m. Conformably overlies: Hampton Sandstone.||||||
14596|Ooldea Sand|44695|5|Briefly described|Map Legend|Eocene|Eocene|(Middle-Late Eocene)||||||
14596|Ooldea Sand|60953|5|Briefly described|Map Legend|Eocene|Paleocene|Aeolian quartz sand, coastal dunes. Geological Province: Eucla Basin.||||||
14596|Ooldea Sand|61108|5|Briefly described|map legend|Eocene|Eocene|Aeolian quartz sand. Coastal dune trends shown. Geological Province: Eucla Basin.||||||
14596|Ooldea Sand|61234|5|Briefly described|p7 Fig. 4|Late Eocene|Middle Eocene|Geological Province: Eucla Basin.||||||
14596|Ooldea Sand|61839|5|Briefly described|p227|Eocene|Eocene|Coastal barrier sands.  Geological Province: Gawler Craton. Shown as two seperate units, one Middle - Late Eocene in part laterally equivalent to the Barton Sand, the other, Ooldea Sand?,  ~ Middle Miocene, laterally equivalent ot the Yarle Sandstone.||||||05-DEC-13
14596|Ooldea Sand|61856|6|Mentioned|p300 Fig.2, p311, p316|Middle Eocene|Middle Eocene|In this article, this unit is split with the naming of a new unit, the Barton Sand, which formed in a separate barrier system.|||||Predominantly medium-grained poorly cemented sand with aeolian frosting features.|
14596|Ooldea Sand|64646|6|Mentioned|p23 Fig. 3, p24 Fig. 4|Miocene|Eocene|Geological Province: Eucla Basin.||||||08-FEB-10
14596|Ooldea Sand|65194|6|Mentioned|p164, p171|Eocene|Eocene|Shoreline deposits.||||||
14596|Ooldea Sand|66131|6|Mentioned|p242 Fig.2|Eocene|Eocene|Late Eocene in age (from p.242 Fig.2 - stratigraphic correlation chart).||||||
14596|Ooldea Sand|67462|5|Briefly described|Map legend.|||Eucla Basin.||||||
14596|Ooldea Sand|67921|5|Briefly described|Map legend|Eocene|Eocene|Found in the Ooldea, Barton and Paling Ranges. Subcrop and minor outcrop.|||||Very fine to medium-grained, moderately to well sorted aeolian quartz sand, partly spicule-bearing.|
14596|Ooldea Sand|68715|6|Mentioned|p30 Fig.5|Miocene|Eocene|Bunda Plateau, Eucla Basin.||||||
14596|Ooldea Sand|69598|6|Mentioned|p9|Early Oligocene|Late Eocene|||||||
14596|Ooldea Sand|69648|4|Described|p4,p6 Fig.3,p21,p23,p29,p36, map legend|Eocene|Eocene|Eucla Basin. Age: Middle to Late Eocene estimated. Thickness: at least 112 m. Possible localised reworking. Coastal barriers of moderate to high energy. Hampton Sandstone, Ooldea Sand, Yarle Sandstone are source of sand for Tertiary coastal sand units (including Wintrena Formation). Prospective for heavy mineral sand deposits.||Burdunga Subgroup||With conformably underlying Hampton Sandstone, overlies Pidinga Formation; overlain by mobile Great Victoria Desert sands (~10-30 m) - boundary type uncertain.|Predominantly medium-grained quartz sand; also very fine (minor) and coarse grained, good roundness, clean to slightly clayey, poorly to moderately consolidated; trace to minor heavy mineral sands (zircon, leucoxene, rutile, ilmentire, tourmaline).|
14596|Ooldea Sand|69649|6|Mentioned|p31,|Eocene|Eocene|Eucla Basin.||||||
14596|Ooldea Sand|70337|5|Briefly described|Map legend.|Pleistocene|Eocene||||||Sand, medium-grained, quartz, well-sorted, well rounded, frosted grains, trace quantities of heavy minerals. Aeolian dunes.|
14596|Ooldea Sand|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sand|
14596|Ooldea Sand|73111|5|Briefly described|Map legend.|Eocene|Eocene|Subcrop and minor outcrop. Is overlain by un-named indurated, red-brown to orange calcareous aeolian sand.|||||Very fine- to medium-grained, moderately to well-sorted aeolian quartz sand of the Ooldea, Barton and Paling Ranges, partly spicule-bearing.|
14640|Oraparinna Shale|22766|5|Briefly described|Fig.2 p561|Early Cambrian|Early Cambrian|||||||
14640|Oraparinna Shale|23818|4|Described|p87 Fig.33, p91|Cambrian|Cambrian|Of the Hawker Group. Contains trilobites and brachipods.||||||
14640|Oraparinna Shale|23981|5|Briefly described|p8-9 Fig. 4, p10 Fig. 5|Early Cambrian|Early Cambrian|Overlies Mernmerna Formation (transitionally); underlies Narina Greywacke; interfingers with Moorowie Formation. Geological Province: Arrowie Basin. See also p52 Fig. 20, p64.||||||15-FEB-07
14640|Oraparinna Shale|24176|5|Briefly described|p16, p23 Tb. 1|Cambrian|Cambrian|Green carbonaceous siltstones.  Overlain by and intertongued with Narina Greywacke.  Max. thickness: 150m.  Geological Province: Mount Painter Province.||||||
14640|Oraparinna Shale|24465|5|Briefly described|p345 Fig.2|Early Cambrian|Early Cambrian|Of the Hawker Group.  Geological Province: Arrowie Basin.||||||19-JAN-05
14640|Oraparinna Shale|29780|4|Described|p108|||||||||
14640|Oraparinna Shale|29929|6|Mentioned|Fig.1|||||||||
14640|Oraparinna Shale|30051|6|Mentioned|p25|||Lower Cambrian age.||||||
14640|Oraparinna Shale|30176|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
14640|Oraparinna Shale|30198|6|Mentioned|p96|||Refers to aquifers and lithology on Table 2||||||
14640|Oraparinna Shale|30801|6|Mentioned|p5|||Table P5-6||||||
14640|Oraparinna Shale|30802|5|Briefly described|p11|||Cambrian age||||||
14640|Oraparinna Shale|30807|6|Mentioned|p102|||Suggested map symbol||||||
14640|Oraparinna Shale|31539|6|Mentioned|p33|||Cambrian. See also Fig. 8, 17, 28||||||
14640|Oraparinna Shale|31706|6|Mentioned|p633|||Cambrian correlation chart||||||
14640|Oraparinna Shale|32669|6|Mentioned|p523|||L.Cambrian||||||
14640|Oraparinna Shale|33474|6|Mentioned|Fig.3|||||||||
14640|Oraparinna Shale|33932|4|Described|p17|||||||||
14640|Oraparinna Shale|33934|4|Described|Fig.2|||L. Camb.||||||
14640|Oraparinna Shale|34185|6|Mentioned|p129|||||||||
14640|Oraparinna Shale|34269|6|Mentioned|Table 1|||||||||
14640|Oraparinna Shale|34612|4|Described|p91|||Cambrian||||||
14640|Oraparinna Shale|35075|6|Mentioned|p77|||||||||
14640|Oraparinna Shale|35255|6|Mentioned|Fig.8|||||||||
14640|Oraparinna Shale|35395|6|Mentioned|p102|||Stratigraphy||||||
14640|Oraparinna Shale|35835|6|Mentioned|p198|||||||||
14640|Oraparinna Shale|36198|6|Mentioned|Table I.1|||Misspelling?[of what?CEBMar95]||||||
14640|Oraparinna Shale|36495|6|Mentioned|p117|||||||||
14640|Oraparinna Shale|36525|6|Mentioned|Fig.4|||||||||
14640|Oraparinna Shale|37802|6|Mentioned|Fig.2|||||||||
14640|Oraparinna Shale|38068|6|Mentioned|p69|||||||||
14640|Oraparinna Shale|40431|6|Mentioned|p12|||||||||
14640|Oraparinna Shale|40672|6|Mentioned|Fig.2|||||||||
14640|Oraparinna Shale|40831|6|Mentioned|Fig.2|||||||||
14640|Oraparinna Shale|40914|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
14640|Oraparinna Shale|41457|6|Mentioned|Fig.1|||||||||
14640|Oraparinna Shale|41496|5|Briefly described|p52|||||||||
14640|Oraparinna Shale|41526|6|Mentioned|p61|||||||||
14640|Oraparinna Shale|41996|6|Mentioned|p2|||||||||
14640|Oraparinna Shale|42011|6|Mentioned|Fig.2 P458|||||||||
14640|Oraparinna Shale|42192|6|Mentioned|p171|||||||||
14640|Oraparinna Shale|42213|5|Briefly described|p474|||See also Fig.2||||||
14640|Oraparinna Shale|42222|6|Mentioned|Table 1 P5|||||||||
14640|Oraparinna Shale|42226|6|Mentioned|p231|||||||||
14640|Oraparinna Shale|42233|6|Mentioned|Fig.1 P248|||||||||
14640|Oraparinna Shale|42266|6|Mentioned|Fig.2 P292|||||||||
14640|Oraparinna Shale|42272|6|Mentioned|p413|||||||||
14640|Oraparinna Shale|42440|6|Mentioned|Fig.2 P602|||||||||
14640|Oraparinna Shale|42458|5|Briefly described|p698|||||||||
14640|Oraparinna Shale|42573|5|Briefly described|Fig.1 P190|||||||||
14640|Oraparinna Shale|43759|6|Mentioned|p452|||||||||
14640|Oraparinna Shale|43781|6|Mentioned|p4||Early Cambrian|||||||
14640|Oraparinna Shale|43845|6|Mentioned|Fig4 p44|||||||||12-JUL-16
14640|Oraparinna Shale|44133|5|Briefly described|p4 Fig. 7.2, 17|Early Cambrian|Early Cambrian|Geological Province: Arrowie Basin.||||||
14640|Oraparinna Shale|44659|5|Briefly described|map legend||Early Cambrian|L.Cambrian, lithology.||||||
14640|Oraparinna Shale|45102|6|Mentioned|p46|||See also P47||||||
14640|Oraparinna Shale|60418|5|Briefly described|p135|Early Cambrian|Early Cambrian|Of the Hawker Group. Geological Province: Arrowie Basin of Adelaide Geosyncline.||||||
14640|Oraparinna Shale|60889|4|Described|p245 Fig.2, p249, p251-4|Early Cambrian|Early Cambrian|Thickness: 200 m. Transgressive. Arrowie Basin. Moorowie Syncline.||Hawker Group||Overlies Bunkers Sandstone. Is overlain by Moorowie Formation and upper Wilkawillina Limestone. Intertongues with Narina Greywacke.|Potential source rocks.|21-SEP-17
14640|Oraparinna Shale|60959|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of the Hawker Group. Khaki-green silty shale becoming calcareous upwards. Abundant limestone concretions.||||||
14640|Oraparinna Shale|60990|5|Briefly described|p83 Fig.2 |Botoman|Botoman|Flinders Ranges.||Hawker Group.||||
14640|Oraparinna Shale|62592|5|Briefly described|p50 Table 5.1.|Early Cambrian|Early Cambrian|Adelaide Geosyncline.||Topmost unit in Hawker Group.||Overlies Mern Merna Formation.|Siltstone.|
14640|Oraparinna Shale|62783|6|Mentioned|p2 Fig.1|||||||||
14640|Oraparinna Shale|62784|5|Briefly described|p8 Fig.1|Cambrian|Cambrian|Arrowie Basin. Upper unit of Hawker Group, overlying Bunkers Sandstone. Overlain by Edeowie Limestone Member of Billy Creek Formation..||||||
14640|Oraparinna Shale|63447|5|Briefly described|p962,p963 Fig.2|Early Cambrian|Early Cambrian|Includes tabulate corals in bioherms at Ten Mile Creek and Moorowie Mine. Also trilobite and echinoderm fragments and archaeocyaths||Hawker Group||Lateral equivalent in part to Ajax Limestone, Mernmerna Formation, Narina Greywacke, upper Wilkawillina Limestone. Overlain by Billy Creek Formation.||
14640|Oraparinna Shale|63569|4|Described|pp116-120, p122|Cambrian|Cambrian|Arrowie Basin, Adelaide Geosyncline. Contains rich assemblage of silicified Estaingia occipitospina trilobites in uppermost 4 m siltstone.||Unit in Hawker Group.||Overlies Bunkers Sandstone. Is unconformably overlain by Edeowie Limestone Member, at least locally.|Fissile green-, grey- and buff-coloured shales, limestone concretions common; minor buff-coloured siltstone with abundant trilobite and mollusc fossils.|
14640|Oraparinna Shale|64829|5|Briefly described|p1084-5 Figs.1,  2|Early Cambrian|Early Cambrian|||||||07-FEB-11
14640|Oraparinna Shale|65313|6|Mentioned|p577, p576 Fig. 5, p578 Fig. 6|Early Cambrian|Early Cambrian|~200 degrees burial temperature.||Of Hawker Group.||||26-MAR-12
14640|Oraparinna Shale|65375|5|Briefly described|p33.|Early Cambrian|Early Cambrian|||Unit in Hawker Group.||Overlies Bunkers Sandstone. Is overlain by Narina Greywacke.||
14640|Oraparinna Shale|65625|5|Briefly described|p103 Fig.2|Early Cambrian|Early Cambrian|Lake Frome area.||||Overlies Bunkers Sandstone. Underlies Billy Creek Formation.||18-FEB-11
14640|Oraparinna Shale|65686|5|Briefly described|p411,  p409 Fig 2|Early Cambrian|Early Cambrian|Arrowie Basin. 200m thick.||||Underlies the Moorowie Formation.||07-MAY-12
14640|Oraparinna Shale|65892|4|Described|p7 Fig.3, p9 Fig.4, p28, p29 Fig.14. |Early Cambrian|Early Cambrian|See also p44-45. Arrowie Basin. 200m thick. A transgressive unit. In eastern Nepabunna Trough, intertongues with Narina Greywacke.||Unit in Hawker Group.|Includes Edeowie Limestone Member.|Overlies Bunkers Sandstone and Mermerna Formation.|Khaki shale; few thin carbonate beds towards the top.|
14640|Oraparinna Shale|65925|5|Briefly described|p14 Fig.2.2, Appendix 2.|Early Cambrian|Early Cambrian||||||Calcareous shale.|
14640|Oraparinna Shale|67870|5|Briefly described|p24-25, p33, p36|Cambrian|Cambrian|Potential hydrocarbon source rocks: 3% TOC. Detailed modelling showing fraction of kerogen transformed, and early oil and gas expulsion (nil).|||||Organic-rich siltstone (2-3%) and limestone (1-2%).|
14640|Oraparinna Shale|68735|5|Briefly described|p233 Fig.2, p234, p235 Fig.3|Early Cambrian|Early Cambrian|Arrowie Basin.||Of the Hawker Group.||Underlain and interfingered by the  Mernmerna Formation. Overlain by the Narina Greywacke. Overlain by the Edeowie Limestone Member.|Comprises khaki shales and siltstones.|
14640|Oraparinna Shale|68993|6|Mentioned|p544 Fig.1|Early Cambrian|Early Cambrian|Arrowie Basin.||Of the Hawker Group.||||
14640|Oraparinna Shale|70833|5|Briefly described|p200-201|Series 2|Series 2|Of Arrowie Basin.||Unit of Hawker Group.||Uppermost unit of Hawker Group. Overlain by Billy Creek Formation. Underlain by Mernmerna Formation.||
14640|Oraparinna Shale|70835|5|Briefly described|p335-337, 346, 354|Cambrian|Cambrian|Arrowie Basin, Flinders Ranges. Contains macromollusc fossils.||Hawker Group.||Conformably overlies Mernmerna Formation or Bunkers Sandstone. Is overlain by Edeowie Limestone. Locally abuts Upper Wilkawillina Limestone.|Lower 38m comprises fissile shales and fist-sized limestone concretions, overlain by 4m of buff-coloured siltstones.|
14640|Oraparinna Shale|71102|5|Briefly described|p242,244-247,251,254,267,269|Series 2|Series 2|Of Arrowie Basin. Intersection sections: 10MS (10 Mile South, Bunkers Graben), BHG (Bullock Head Gap, SW Arrowie Syncline)||||Overlain by Billy Creek Formation. Underlain by Mernerna Formation|Recessive, kahki-green silty shale.|05-SEP-19
14640|Oraparinna Shale|72429|5|Briefly described|p949, p958, p967-968, p970, p972|Cambrian|Cambrian|Mount Chambers Gorge, eastern Flinders Ranges. Green grey shales are similar to those found in Brillig Catch Member. Capped by microbial laminites and dolomitic mudstones of the Edeowie Limestone Member.||Hawker Group||Equivalent to the Moorowie Formation (in part). Interfingers with the Wilkawillina Limestone.|Shale and interbedded biostromal archaeocyathan limestones.|
14640|Oraparinna Shale|72449|5|Briefly described|p1, p2 Map Legend|Cambrian|Cambrian|Includes the first trilobites. Shown in image on p1, 'Trilobite from the Oraparinna Shale'. (Courtesy of Jim Gehling; photo 408458)||||Overlies Mernmerna Formation, Bunkers Sandstone and underlies Billy Creek Formation|Khaki-green silty shale with limestone concretions which often contain fossil fragments.|
14640|Oraparinna Shale|73255|6|Mentioned|p534 Fig.2|early Cambrian|early Cambrian|Contains Redlichia takooensis trilobite fossils.||||Overlies the Bunkers Sandstone, underlies the Billy Creek Formation.||
14655|Orroroo Kimberlites|41703|6|Mentioned|p243|||||||||
14657|Orroroo kimberlite|23772|5|Briefly described|p764||Jurassic|Gawler Craton. Age: 170 Ma.||||||
14657|Orroroo kimberlite|40811|4|Described|p321, p320|||||||||
14657|Orroroo kimberlite|41703|6|Mentioned|p243|||||||||
14685|Otway Group|12796|6|Mentioned|p455|||Geological Province: Otway Basin.||||||
14685|Otway Group|13323|5|Briefly described|p392|||Raised to rank of supergroup following introduction of Crayfish Group (Kopsen abd Scholefield 1990) but this caused discontinuity of nomenclature and was considered to have 'limited usefulness' by many (Morton et al 1994). Geol.Prov: Otway Basin.||||||26-JUN-06
14685|Otway Group|13350|5|Briefly described|p95, p106||Early Cretaceous|Geological Province: Otway Basin, Bass and Boobyalla Sub-basins and probably the Sorrell Basin west of Tasmania.||||||29-JAN-07
14685|Otway Group|22495|6|Mentioned|P220|||||||||
14685|Otway Group|22706|6|Mentioned|Fig1,p78|||||||||
14685|Otway Group|22875|4|Described|p25|Early Cretaceous|Late Jurassic|Age: 157-95 Ma.||||||29-JAN-07
14685|Otway Group|22938|6|Mentioned|p233||Early Cretaceous|||||||
14685|Otway Group|22944|5|Briefly described|Fig3|Albian|Tithonian|||||||
14685|Otway Group|23010|6|Mentioned|p333-341||Early Cretaceous|||||||
14685|Otway Group|23041|6|Mentioned|p116||Cretaceous|||||||
14685|Otway Group|23230|5|Briefly described|p39, Table4-1p40|Early Cretaceous||||||||
14685|Otway Group|23239|5|Briefly described|Table1p109, 116||Early Cretaceous|||||||
14685|Otway Group|23241|5|Briefly described|p133, 135, Fig11-3.6p140|Late Cretaceous|Early Cretaceous|||||||
14685|Otway Group|23243|5|Briefly described|Fig11-5.1p170||Late Cretaceous|||||||
14685|Otway Group|23249|6|Mentioned|Fig.1|||of Otway Basin.||||||
14685|Otway Group|23307|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|||||||
14685|Otway Group|23357|5|Briefly described|52|Early Cretaceous|Early Cretaceous|||||||
14685|Otway Group|23372|4|Described|p251 Fig3,p249|Albian|Barremian|Of Bass Basin.||||||01-JUL-08
14685|Otway Group|23427|5|Briefly described|Table 11.2 p418.|||||||||
14685|Otway Group|23537|5|Briefly described|p 440|||||||||
14685|Otway Group|23778|5|Briefly described|p660|Early Cretaceous|Early Cretaceous|Overlain by Eastern View Group. In the Otway Basin.||||||29-JAN-07
14685|Otway Group|23792|6|Mentioned|Fig.B13||Early Cretaceous|Forms basement for Sandy Cape Sub-basin. See also Otway Supergroup.||||||
14685|Otway Group|23818|4|Described|p150, 161|Late Jurassic|Late Jurassic|Geological Province: Otway Basin. Age: 153+/-5 Ma. Max. thickness: >10 000 ft. Overlain by Sherbrook Group.||||||29-JAN-07
14685|Otway Group|23824|6|Mentioned|p102|||Geological Province: Otway Basin.||||||
14685|Otway Group|23830|5|Briefly described|Fig. 6|Early Cretaceous|Late Jurassic|Geological Province: Gambier Embayment, Otway Basin.||||||24-JAN-06
14685|Otway Group|23909|5|Briefly described|p291|Early Cretaceous|Early Cretaceous|Geological Province: Otway Basin.||||||
14685|Otway Group|23911|5|Briefly described|p95 Fig. 9B|Albian|Late Jurassic|Geological Province: Otway Basin.||||||
14685|Otway Group|24002|5|Briefly described|p236|Cretaceous|Cretaceous|||||||
14685|Otway Group|24038|5|Briefly described|p438 Fig.1|Early Cretaceous|Early Cretaceous|||||||
14685|Otway Group|24055|4|Described|p71|Early Cretaceous|Jurassic|Geological Basin: Otway Basin.||||||
14685|Otway Group|24056|4|Described|p84|Early Cretaceous|Jurassic|Max. thickness: 3500m.  Geological Basin: Otway Basin.||||||
14685|Otway Group|24085|6|Mentioned|p42 Tb.2|Early Cretaceous|Early Cretaceous|||||||
14685|Otway Group|24113|5|Briefly described|p284|||See also p282 Tb 2.||||||
14685|Otway Group|24160|6|Mentioned|p19|Early Cretaceous|Early Cretaceous|Gellibrand, northern Otway Ranges. Hosts bentonite deposits.|||||Includes arkose, mudstone and shale.|
14685|Otway Group|24200|6|Mentioned|p416|||||||||
14685|Otway Group|24238|5|Briefly described|p8|Early Cretaceous|Jurassic|Geological Province: Otway Basin.||||||
14685|Otway Group|24323|6|Mentioned|p144|||Geological Province: Otway Basin||||||
14685|Otway Group|24453|5|Briefly described|p808, p809 Fig.2|Albian|Late Jurrasic|Geological Province: Otway Basin.||||||07-FEB-11
14685|Otway Group|24455|5|Briefly described|p327|Early Cretaceous|Early Cretaceous|Bears dinosaur remains.  Transgressively overlapped by Pebble Point Formation.||||||
14685|Otway Group|24551|4|Described|p240 Fig. 9.2, p247|Cretaceous|Late Jurassic|Duddy (1983) proposed to replace this name with Otway Formation due to objections to the term 'group'; also, Otway Supergroup was proposed (Kopsen and Scholefield 1990) but rejected due to its limited use.||||||29-JAN-07
14685|Otway Group|24561|5|Briefly described|p27|||Geological Province: Otway and Bass Basins. Includes volcanogenic sediments.||||||04-FEB-08
14685|Otway Group|24562|5|Briefly described|p20, 91|Early Cretaceous|Early Cretaceous|Overlies: Pretty Hill Formation.  Geological Province: Otway Basin.||||||
14685|Otway Group|29591|6|Mentioned|p92|||||||||
14685|Otway Group|29697|6|Mentioned|Fig.11|||||||||
14685|Otway Group|29823|6|Mentioned|p14|||||||||
14685|Otway Group|29856|6|Mentioned|p36|||||||||
14685|Otway Group|29877|6|Mentioned|p33|||||||||
14685|Otway Group|30018|5|Briefly described|p15|||||||||
14685|Otway Group|30499|6|Mentioned|p92|||Stratigraphy||||||
14685|Otway Group|30512|6|Mentioned|p51|||||||||
14685|Otway Group|30522|6|Mentioned|Map legend|Early Cretaceous|Jurassic|Jurassic-Lower Cretaceous||||||
14685|Otway Group|30539|6|Mentioned|p7|||Late Albian angiosperms||||||
14685|Otway Group|30576|6|Mentioned|Table 1|||||||||
14685|Otway Group|30578|6|Mentioned|p4|||||||||
14685|Otway Group|30580|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
14685|Otway Group|30675|5|Briefly described|p253|||Lithology and radioactivity||||||29-JAN-07
14685|Otway Group|30754|5|Briefly described|p4|||Stratigraphic divisions. See also P12,24||||||
14685|Otway Group|30905|4|Described|p148|||||||||
14685|Otway Group|30928|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
14685|Otway Group|30929|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
14685|Otway Group|30932|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
14685|Otway Group|30990|6|Mentioned|p125|||Refers Edwards & Barkes (1943)||||||
14685|Otway Group|31001|6|Mentioned|p7|||||||||
14685|Otway Group|31010|6|Mentioned|p51|||||||||
14685|Otway Group|31036|6|Mentioned|Table 9-1|||See also P215||||||
14685|Otway Group|31160|6|Mentioned|p77|||See also P78||||||
14685|Otway Group|31202|5|Briefly described|p218|||Unconformity with Sherbrook Gp. and rift formation..||||||29-JAN-07
14685|Otway Group|31212|6|Mentioned|p318|||Gravity data. L. Cretaceous. See also P320||||||
14685|Otway Group|31242|6|Mentioned|p12|||Refers hydrogeology||||||
14685|Otway Group|31372|6|Mentioned|p2|||See also P9||||||
14685|Otway Group|31424|4|Described|p20|||See also p7. Described from core.||||||29-JAN-07
14685|Otway Group|31510|6|Mentioned|p12|||See also Table 1.||||||
14685|Otway Group|31534|6|Mentioned|p363|||See also Table 19-3. L.Cretaceous||||||
14685|Otway Group|31616|6|Mentioned|p202|||L.Cret.||||||
14685|Otway Group|31624|6|Mentioned|p93|||See also P96. L.Cret.||||||
14685|Otway Group|31625|6|Mentioned|Fig. 5.2|||L.Cret||||||
14685|Otway Group|31629|6|Mentioned|Fig. 5.1|||L.Cret.||||||
14685|Otway Group|31714|6|Mentioned|Fig. 8|||||||||
14685|Otway Group|31920|4|Described|p49|||L.Cret. See also Fig.3-2||||||
14685|Otway Group|31923|6|Mentioned|p16|||||||||
14685|Otway Group|32162|4|Described|p58|||Petroleum apsect||||||
14685|Otway Group|32167|6|Mentioned|p.340||Early Cretaceous|||||||
14685|Otway Group|32168|6|Mentioned|p32|||||||||
14685|Otway Group|32232|6|Mentioned|p19|||||||||
14685|Otway Group|32344|6|Mentioned|Fig.2|||||||||
14685|Otway Group|32712|6|Mentioned|Table 1|||||||||
14685|Otway Group|32841|6|Mentioned|p6|||||||||
14685|Otway Group|32852|6|Mentioned|p9|||||||||
14685|Otway Group|32894|4|Described|p286|||U.Jur.-L.Cret. See also p293.||||||29-JAN-07
14685|Otway Group|32897|6|Mentioned|p177|||L.Cret.||||||
14685|Otway Group|32898|6|Mentioned|Table 2-1|||||||||
14685|Otway Group|32899|4|Described|p164|||See also pp165-176.||||||29-JAN-07
14685|Otway Group|33135|5|Briefly described|p17|||||||||
14685|Otway Group|33155|5|Briefly described|p114|||||||||
14685|Otway Group|33165|6|Mentioned|Chart|||Correlation chart only||||||
14685|Otway Group|33228|6|Mentioned|p2|||||||||
14685|Otway Group|33229|4|Described|p242|||Jur.- L.Cret.||||||
14685|Otway Group|33230|6|Mentioned|Encl.12.1|||L.Cret.||||||
14685|Otway Group|33236|5|Briefly described|p19|||L.Cret. See also p22.||||||29-JAN-07
14685|Otway Group|33240|6|Mentioned|p2|||||||||
14685|Otway Group|33319|6|Mentioned|p178|||Strat.||||||
14685|Otway Group|33354|6|Mentioned|p187|||L.Cret.||||||
14685|Otway Group|33412|6|Mentioned|p218|||L.Cret.||||||
14685|Otway Group|33602|6|Mentioned|Table 1|||||||||
14685|Otway Group|33627|6|Mentioned|p595|||||||||
14685|Otway Group|33663|6|Mentioned|p3|||||||||
14685|Otway Group|33936|6|Mentioned|Fig.6|||U.Jur. - L.Cret.||||||
14685|Otway Group|33940|4|Described|p387|||L.Cret. See p400.||||||29-JAN-07
14685|Otway Group|33943|6|Mentioned|p378|||L.Cret.||||||
14685|Otway Group|34001|6|Mentioned|p14|||In Hindaugh No.1 Well||||||
14685|Otway Group|34063|6|Mentioned|p3|||L.Cret. Table||||||
14685|Otway Group|34148|6|Mentioned|p10|||Lower Cretaceous. See also PP272,285,286.||||||
14685|Otway Group|34191|6|Mentioned|Map legend|Albian|Neocomian|Neocomian - Albian||||||
14685|Otway Group|34308|6|Mentioned|Fig.86|||||||||
14685|Otway Group|34343|5|Briefly described|p96|||||||||
14685|Otway Group|34611|6|Mentioned|p161|||Mesozoic. Non marine.||||||
14685|Otway Group|34928|5|Briefly described|p55|||||||||
14685|Otway Group|34966|6|Mentioned|p364|||||||||
14685|Otway Group|34967|6|Mentioned|p347|||||||||
14685|Otway Group|34987|5|Briefly described|p170|||||||||
14685|Otway Group|34988|6|Mentioned|Table 9.4|||||||||
14685|Otway Group|34993|6|Mentioned|p302|||||||||
14685|Otway Group|35013|4|Described|p390|||||||||
14685|Otway Group|35066|6|Mentioned|p203|||||||||
14685|Otway Group|35112|6|Mentioned|Table 1|||||||||
14685|Otway Group|35151|6|Mentioned|p150|||||||||
14685|Otway Group|35274|6|Mentioned|p421|||||||||
14685|Otway Group|35276|6|Mentioned|p231|||||||||
14685|Otway Group|35290|6|Mentioned|p23|||||||||
14685|Otway Group|35712|6|Mentioned|Table 6|||||||||
14685|Otway Group|35722|6|Mentioned|p3|||Stratigraphy.||||||
14685|Otway Group|36366|6|Mentioned|p5|||||||||
14685|Otway Group|36499|3|Fully described|p17|||||||||
14685|Otway Group|36553|6|Mentioned|p364|||||||||
14685|Otway Group|36824|6|Mentioned|p65|||||||||
14685|Otway Group|36913|6|Mentioned|p78|||See also Fig.4.||||||
14685|Otway Group|37065|5|Briefly described|p42|||||||||
14685|Otway Group|37129|5|Briefly described|p359|||||||||
14685|Otway Group|37131|6|Mentioned|p364|||||||||
14685|Otway Group|37548|6|Mentioned|p131|||||||||
14685|Otway Group|38008|6|Mentioned|p1|||||||||
14685|Otway Group|38068|4|Described|p72|||||||||
14685|Otway Group|38221|6|Mentioned|Fig.4|||Otway Basin||||||
14685|Otway Group|38625|6|Mentioned|p271|||||||||
14685|Otway Group|38928|6|Mentioned|p12|||||||||
14685|Otway Group|39022|6|Mentioned|p397|||||||||
14685|Otway Group|39077|6|Mentioned|Table 2|||||||||
14685|Otway Group|39211|6|Mentioned|Fig.45|||||||||
14685|Otway Group|39666|6|Mentioned|p111|||||||||
14685|Otway Group|40003|5|Briefly described|p43|||See also Fig.10||||||
14685|Otway Group|40560|6|Mentioned|p4|||||||||
14685|Otway Group|40641|4|Described|p295|||||||||
14685|Otway Group|40947|6|Mentioned|p3|||||||||
14685|Otway Group|41016|5|Briefly described|p213|||||||||
14685|Otway Group|41057|6|Mentioned|p60|||||||||
14685|Otway Group|41124|4|Described|p255|||||||||
14685|Otway Group|41171|6|Mentioned|p167|||||||||
14685|Otway Group|41185|5|Briefly described|p175|||See also Fig.4||||||
14685|Otway Group|41201|6|Mentioned|p7|||||||||
14685|Otway Group|41269|5|Briefly described|p244|||||||||
14685|Otway Group|41318|6|Mentioned|p182|||||||||
14685|Otway Group|41426|6|Mentioned|p3|||||||||
14685|Otway Group|41487|6|Mentioned|p624|||||||||
14685|Otway Group|41521|6|Mentioned|p239|||||||||
14685|Otway Group|41552|6|Mentioned|p459|||||||||
14685|Otway Group|41642|4|Described|p224|||See also p 217?||||||
14685|Otway Group|41701|6|Mentioned|Map legend|Cretaceous||||||||
14685|Otway Group|41704|5|Briefly described|p99|||See also p100.||||||29-JAN-07
14685|Otway Group|41706|6|Mentioned|p145|||||||||
14685|Otway Group|41714|6|Mentioned|p301|||||||||
14685|Otway Group|41715|6|Mentioned|p312|||||||||
14685|Otway Group|41726|5|Briefly described|p420|||||||||
14685|Otway Group|41769|4|Described|p9|||||||||
14685|Otway Group|41797|5|Briefly described|p223|||||||||
14685|Otway Group|41818|6|Mentioned|p40|||||||||
14685|Otway Group|41848|6|Mentioned|p377|||Age Lower Cretaceous||||||
14685|Otway Group|41849|6|Mentioned|p413|||||||||
14685|Otway Group|41868|4|Described|p531|||||||||
14685|Otway Group|41936|6|Mentioned|p77|||||||||
14685|Otway Group|42152|6|Mentioned|Fig.2 P4|||||||||
14685|Otway Group|42153|6|Mentioned|p351|||See also Table 1||||||
14685|Otway Group|42184|6|Mentioned|Fig.2 P348|||||||||
14685|Otway Group|42318|5|Briefly described|p5|||||||||
14685|Otway Group|42357|6|Mentioned|p11|||||||||
14685|Otway Group|42361|4|Described|p4|||||||||
14685|Otway Group|42415|5|Briefly described|p177|||Otway Basin||||||
14685|Otway Group|42423|5|Briefly described|p327|||||||||
14685|Otway Group|42452|5|Briefly described|Map legend|Albian|Neocomian|||||||
14685|Otway Group|42453|4|Described|p10|Albian|Neocomian|||||||
14685|Otway Group|42524|5|Briefly described|p27|||||||||
14685|Otway Group|42545|6|Mentioned|p4|||Otway Basin||||||
14685|Otway Group|42555|5|Briefly described|p284|||||||||
14685|Otway Group|42599|5|Briefly described|Fig.3 P614|||||||||
14685|Otway Group|42635|6|Mentioned|p88|||||||||
14685|Otway Group|42827|3|Fully described|p217|||||||||
14685|Otway Group|42863|5|Briefly described|Fig.14|||Variation on Victorian unit.||||||
14685|Otway Group|42966|6|Mentioned|p68|||||||||
14685|Otway Group|43171|6|Mentioned|8|Early Cretaceous|Late Jurassic|Age: 105-155Ma||||||
14685|Otway Group|43208|5|Briefly described|map legend|Albian|Oxfordian|||||||
14685|Otway Group|43219|5|Briefly described|Fig.3,p6.|Albian|Oxfordian|||||||
14685|Otway Group|43590|4|Described|p7|Early Cretaceous|Late Jurassic|||||||
14685|Otway Group|43604|6|Mentioned|p144,Fig.1||Cretaceous|||||||
14685|Otway Group|43660|6|Mentioned|p9||Early Cretaceous|||||||
14685|Otway Group|43686|5|Briefly described|p233||Early Cretaceous|||||||
14685|Otway Group|43702|6|Mentioned|Fig.2,p398||Early Cretaceous|||||||
14685|Otway Group|43705|6|Mentioned|p14||Cretaceous|||||||
14685|Otway Group|43733|6|Mentioned|Fig.1.10,p24|||||||||
14685|Otway Group|43783|6|Mentioned|Fig14, p11|||||||||
14685|Otway Group|43784|6|Mentioned|Fig10, p12|||||||||
14685|Otway Group|43814|6|Mentioned|Fig.3,p115|||||||||
14685|Otway Group|43937|5|Briefly described|Map Legend|Aptian|Kimmeridgian|||||||
14685|Otway Group|44135|5|Briefly described|p46, p47|Early Cretaceous|Early Cretaceous|Age: 126-103Ma.Thickness: 1200m.  Geological province: Otway, Bass and Durroon Basins. Rift-fill succession of immature volcaniclastic lithic sandstone, siltstone, rare conglomerate and thin coal seams.||||||07-DEC-09
14685|Otway Group|46909|6|Mentioned|Fig.1|||||||||
14685|Otway Group|46970|6|Mentioned|Fig.17|||||||||
14685|Otway Group|46988|6|Mentioned|p201|||||||||
14685|Otway Group|48581|4|Described|p26-31|||See also p1,2,16,35,40. Fig.6,Pl.2. (J54-12).||||||
14685|Otway Group|48631|14|Not recorded|p7|||non-marine, Otway Basin.||||||
14685|Otway Group|48911|5|Briefly described|p11|||Formations in the group.||||||
14685|Otway Group|48977|5|Briefly described|p26|||See also P1 & Table 3. Lower Cret.||||||
14685|Otway Group|49060|5|Briefly described|Fig.33|||||||||
14685|Otway Group|50043|6|Mentioned|p2, p10, 12|Early Albian|Late Aptian||||Includes Eumeralla Formation.|||27-MAR-12
14685|Otway Group|50154|4|Described|p25, p108, p131|Cretaceous|Cretaceous|Age: ca. 140-100 Ma. Nonconformably overlies the Dergholm Granite.||||||05-JAN-16
14685|Otway Group|50155|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|Includes Eumeralla Formation.||||||27-OCT-08
14685|Otway Group|50156|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|Includes Eumeralla Formation.||||||27-OCT-08
14685|Otway Group|50157|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|Includes Eumeralla Formation||||||
14685|Otway Group|50158|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|Includes Eumeralla Formation||||||24-JUN-04
14685|Otway Group|50159|5|Briefly described|Map Legend|||Includes Eumeralla Formation.||||||29-JAN-07
14685|Otway Group|50160|5|Briefly described|Map Legend|||Includes Eumeralla Formation||||||16-JUN-04
14685|Otway Group|50161|5|Briefly described|Map Legend|||Includes Eumeralla Formation||||||
14685|Otway Group|50162|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|Includes Eumeralla Formation||||||22-JUN-04
14685|Otway Group|50163|5|Briefly described|Map Legend|Cretaceous|Cretaceous|||||||
14685|Otway Group|50164|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|Overlies Nangeela Formation. Overlain by Renmark Group. Fluvial; sandstone, siltstone, minor conglomerate, coal.||||||25-JUN-04
14685|Otway Group|50594|5|Briefly described|p27|Early Cretaceous|Late Jurassic|Geological Province: Otway Basin.||||||
14685|Otway Group|60299|5|Briefly described|p228 Tb.5|Cretaceous|Cretaceous|Age: 110/115 Ma. Palaeopole position given.||||||
14685|Otway Group|60421|5|Briefly described|p408 Fig. 1, 409, 411|Cretaceous|Cretaceous|Sedimentary.||||||
14685|Otway Group|60451|5|Briefly described|p95 Fig. 61|||||||||
14685|Otway Group|60563|5|Briefly described|p45|Cretaceous|Cretaceous|Geological Province: Otway Basin.||||||
14685|Otway Group|61017|5|Briefly described|p5|Albian|Oxfordian|Includes the Crayfish Subgroup. Geological Province: Otway Basin.||||||07-FEB-11
14685|Otway Group|61181|5|Briefly described|p16, p25, p133|Early Cretaceous|Early Cretaceous|Bentonite occurs interbedded within the sediments which comprise arkose, mudstone and shale in the Gellibrand area. Rare ligneous mudstone and thin coal seams are also present. Unconformably overlain by the Jan Juc Formation.||||||
14685|Otway Group|61182|4|Described|p10, p35|Early Cretaceous|Late Jurassic|Comprises Casterton, Pretty Hill and Eumeralla Formations. Unconformably overlain by Sherbrook Group. Geological Province: Otway Basin. Sequence of basalt, pyroclastics, lithic sandstone, siltstone and shale. Age: 157-97Ma.||||||
14685|Otway Group|61328|6|Mentioned|p116-117|Early Cretaceous|Early Cretaceous|Age: ~95Ma.||||||
14685|Otway Group|61336|6|Mentioned|p(i)|||Geological Province: Otway Basin.||||||07-FEB-11
14685|Otway Group|61470|5|Briefly described|p28 Fig. 5|Albian|Oxfordian|Includes the Casterton Formation, Crayfish Subgroup (Pretty Hill and Laira Formations and Katnook Sandstone) and Eumeralla Formation. Geological Province: Otway Basin.||||||12-OCT-05
14685|Otway Group|61552|6|Mentioned|p584.|||Otway Basin. This is the western rift equivalent to the Strzelecki Group in the Gippsland Basin.||||||
14685|Otway Group|61607|6|Mentioned|p5 Fig. 2|Early Cretaceous|Early Cretaceous|Geological Province: Otway Basin.||||||12-MAR-09
14685|Otway Group|61608|6|Mentioned|p37|||||||||
14685|Otway Group|61624|6|Mentioned|p465|Cretaceous|Late Jurassic|Geological Province: Otway Basin.||||||07-APR-09
14685|Otway Group|61625|6|Mentioned|p476 Fig. 2|||||||||07-FEB-11
14685|Otway Group|61626|5|Briefly described|p487, p486 Fig. 2, p493, p493 Fig. 14|Early Cretaceous|Jurassic|Includes; Casterton, Gletwood Beach and Eumeralla Formations, Windermere and Heathfield Sandstones. Geological Province: Otway Basin.||||||
14685|Otway Group|61628|5|Briefly described|p509 Fig. 3, p510 Fig. 4|Early Cretaceous|Late Jurassic|Includes the Crayfish Subgroup, Casterton and Eumeralla Formations. Geological Province: Otway Basin.||||||
14685|Otway Group|61726|5|Briefly described|p924 Fig.3|Cretaceous|Cretaceous|||||||
14685|Otway Group|61841|6|Mentioned|p242|Cretaceous|Cretaceous|||||||03-JUL-06
14685|Otway Group|62896|6|Mentioned|p88|Mesozoic|Mesozoic|||||||07-FEB-11
14685|Otway Group|63173|5|Briefly described|p341, p342 Fig. 9.2, p351|Early Cretaceous|Late Jurassic|Geological Province: Otway Basin.||||||07-FEB-11
14685|Otway Group|63263|6|Mentioned|p36|||Mentioned as Late Jurassic-mid-Cretaceous correlates.||||||07-FEB-11
14685|Otway Group|63269|5|Briefly described|p604-606, p609, p618, p622-624|Early Cretaceous|Late Jurassic|Otway Basin. Terrestrial source rocks. Details of oils and oil stains in named wells tabulated.|||Crayfish Subgroup; Casterton, Eumeralla Formations.|Is overlain unconformably by Sherbrook Group.||
14685|Otway Group|63445|5|Briefly described|Map legend.|Early Cretaceous|Early Cretaceous||||Eumeralla Formation.|||
14685|Otway Group|63446|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous||||Includes Eumeralla Formation.|||
14685|Otway Group|63740|6|Mentioned|p88|Mesozoic|Mesozoic|||||||07-FEB-11
14685|Otway Group|64535|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Includes Tyers River Subgroup and Eumeralla Formation.||||||22-DEC-08
14685|Otway Group|64539|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Includes Tyers River Subgroup and Eumeralla Formation.||||||22-DEC-08
14685|Otway Group|64540|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Includes Tyers River Subgroup and Eumeralla Formation.||||||22-DEC-08
14685|Otway Group|64605|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Includes Tyers River Subgroup amd Eumeralla Formation.||||||17-NOV-08
14685|Otway Group|64616|5|Briefly described|p141-144, p298|Early Cretaceous|Early Cretaceous|Gippsland Basin. Proposed to replace the "still largely informally used" Strzelecki Group which has the same rift basin sediments. Includes Tyers River Subgroup and Eumeralla Formation.||||||
14685|Otway Group|65107|6|Mentioned|p297 Fig 15|Early Cretaceous|Early Cretaceous|100-105 Ma||||||
14685|Otway Group|65316|5|Briefly described|p596||Early Cretaceous|Basal sedimentary package in the central coast Otway and Gippsland Basins; called the Strzelecki Group in the Gippsland Basin.||||Overlain unconfomably by Eastern View Group.|Volcaniclastic and fluvial sediments.|23-APR-12
14685|Otway Group|65715|5|Briefly described|p9 Tb.6, p10, p37|Cretaceous|Cretaceous|Includes Barwon River Conglomerate and Eumeralla Formation. Early Cretaceous.||||||
14685|Otway Group|65717|6|Mentioned|p10|||Otway Basin. Has strong affinities with the Strzelecki Group in the Gippsland Basin.||||||
14685|Otway Group|65718|6|Mentioned|p11|||Otway Basin.||||||
14685|Otway Group|65973|6|Mentioned|p14||||||Includes the Eumeralla Formation.|||
14685|Otway Group|66002|5|Briefly described|p9 Tb.6, p11, p16|Mesozoic|Mesozoic|Includes Eumeralla Formation. Overlain by Wiridjil Gravel and Moomowroong Sand in places. See discussion in VandenBerg 2009.||||||
14685|Otway Group|66181|5|Briefly described|p310 Fig.5|Albian|Berriasian|Includess the Eumeralla Formation and the Tyers River Subgroup. Unconformably underlies the Latrobe Group.||||||
14685|Otway Group|66244|5|Briefly described|p4.|Early Cretaceous|Early Cretaceous|Name applied by VandenBerg et al. (2006) and VandenBerg (2008) to all the Early Cretaceous clastic sedimentary rocks in the Otway, Bass and Gippsland Basins, thus replacing the Strzelecki Group. Because of its entrenched nature in the petroleum industry, the name (Strzelecki Group) is retained for the Early Cretaceous equivalent of the Otway Group in the Gippsland Basin.||||||
14685|Otway Group|66245|5|Briefly described|p6 Fig.5, p15, p53, pp65-67 Figs.D1-D3.|Early Cretaceous|Late Jurassic|This unit may extend well beyond the shelf edge. The lower part was deposited in a well-developed E - W half graben, with 3 sequences of lacustrine shale basin centre and infilling lacustrine delta facies. During Late Cretaceous, early parts of this unit were uplifted and eroded to form the shallow marine shelf of the Mussel Platform. The top of this unit is used to correlate well logs in this study.|||Includes Casterton and Eumeralla Formations and Crayfish Subgroup.|||
14685|Otway Group|67061|5|Briefly described|p545, p546 Fig.3, p557.|Early Cretaceous|Late Jurassic|Largely non-marine. Up to 3 km of rocks from this and older units were removed during exhumation that accompanied deformation between 100 and 95 Ma.|||Includes Pretty Hill Sandstone and Eumeralla Formation.|Is overlain unconformably by the Eastern View Group.||
14685|Otway Group|67366|6|Mentioned|p103 Fig.2. |Early Cretaceous||||||Is overlain unconformably by Sherbrook Group.||
14685|Otway Group|67367|5|Briefly described|p130, p131 Fig.2. |Early Cretaceous|Late Jurassic|Non-marine sands and shales.|||Includes Casterton and Eumeralla Formations and Crayfish Subgroup.|||
14685|Otway Group|67655|5|Briefly described|p24|Early Cretaceous|Early Cretaceous|Angular unconformity at the top of this group. Geol. Prov: Bass Basin.||||||28-MAY-14
14685|Otway Group|68189|6|Mentioned|p25|||Of the Otway Basin.|||Includes the Casterton Formation and the Eumeralla Formation.|||
14685|Otway Group|68206|6|Mentioned|p27||||||||Contains carbonate concretions.|
14685|Otway Group|69297|5|Briefly described|p79, p97, p99 fig 2.32, p104, p400|Cenomanian|Tithonian|Otway Basin.|||Includes the Crayfish Subgroup and the Eumeralla Formation.|||
14685|Otway Group|69651|5|Briefly described|p10, p12|Early Cretaceous|Late Jurassic|Comprises Crayfish and Eumeralla Supersequences.|||Casterton, Eumeralla Formations; Crayfish Subgroup.|Is overlain unconformably by Sherbrook Group.||
14685|Otway Group|69879|5|Briefly described|p417, p435-436, p462|Albian|Aptian|Otway and Bass Basins. Volcanogenic material may come from a volcanic arc/backarc system along the Lord Howe Rise, or Cape Portland shoshonite complex and/or Cygnet Alkaline Complex. Coal and lacustrine shale provide the main hydrocarbon source rocks in Bass Basin.|||||Non-marine volcanogenic sediments from dacitic volcanism, coal and lacustrine shale.|
14685|Otway Group|70077|5|Briefly described|Nelson: Fig.2; p1-2. Regional: Fig.4; p1|Early Cretaceous|Early Cretaceous|See also Regional: p3, p9. Otway Basin: Gambier Embayment and Voluta Trough. Distal equivalents in the Nelson Sub-basin may be petroleum sources.|||Crayfish Subgroup; Eumeralla, Casterton Formations.|Is overlain by Sherbrook Group.||
14685|Otway Group|70078|5|Briefly described|Northern: Fig.2; p2. Regional: Fig.4|Albian|Albian|Otway Basin. Fluvio-lacustrine, coaly rocks equivalent to this unit in the Sorell Basin are potential hydrocarbon sources.|||Eumeralla Formation.|Is overlain by Sherbrook Group.||
14685|Otway Group|70942|14|Not recorded|p117||Mesozoic|||||||
14685|Otway Group|71419|5|Briefly described|p8 Fig 2, p16 Fig 17|Cretaceous|Cretaceous|Fluvial sediments.|||Includes Eumeralla Formation.|||02-FEB-18
14685|Otway Group|71593|6|Mentioned|p45, p138|||Otway Basin.||||||
14685|Otway Group|73153|6|Mentioned|p287||||||Eumeralla Formation|||
14685|Otway Group|73356|6|Mentioned|p1, p4, p14, p17, p20||||||Eumeralla Formation, Heathfield Sandstone, Windermere Sandstone, Casterton Formation, and Crayfish Subgroup and units therein|||
14685|Otway Group|73357|6|Mentioned|p2 Fig.1.1, p43, p45, p47|Albian|Berriasian|Otway Basin.|||Crayfish Subgroup|||
14685|Otway Group|73383|4|Described|v-vi, p2-4, p6, p11|Cenomanian|Tithonian|Otway Basin. Equivalent to chemostratigraphic sequences S0 to S4.|||Casterton Formation, Crayfish Subgroup, Eumeralla Formation|Underlies Sherbrook Group|Includes lacustrine mudstones and alluvial sandstones with initial basaltic volcanics, fluvial channel sandstones, and fluvial volcanoclastics, lithicarenites, mudstones, coal, fluvial overbank and floodplain deposits.|
14685|Otway Group|73385|5|Briefly described|p4-5, p28|Albian|Tithonian|Otway Basin. Previously referred to as the 'Merino Group'.|||Crayfish Subgroup, Eumeralla Formation, Windermere Sandstone, Hawkesdale Volcanics, Heathfield sandstone|Underlies Sherbrook Group.|Includes lacustrine mudstones and alluvial sandstones with initial basaltic volcanics, fluvial channel sandstones, and fluvial volcanoclastics, lithicarenites, mudstones, coal, fluvial overbank and floodplain deposits.|
14685|Otway Group|73386|4|Described|p1, p4-7, p10, p12, iii, Attachment A1|Albian|Tithonian|Otway Basin. Unconformably overlies Paleozoic basement. Belongs to Retitriletes watherooensis - Phimopollenites pannosus spore pollen zones. Chemostratigraphic division into sequences S0-S4 of Forbes et al. (2020). Top boundary represents a sequence boundary characterised by uplift and erosion during the Cenomanian inversion. Contact with overlying Sherbrook Group varies from conformable or mildly disconformable to unconformable. Wangerrip Group onlaps the Otway Group along northern margin of basin.|||Casterton Formation, Crayfish Subgroup, Eumeralla Formation|Underlies Sherbrook Group|Includes lacustrine mudstones and alluvial sandstones with initial basaltic volcanics, fluvial channel sandstones, volcanoclastics, lithicarenites, mudstones, coal, fluvial overbank and floodplain deposits.|
14685|Otway Group|73505|6|Mentioned|p2, p14|Early Cretaceous|Late Jurassic|||||||
14685|Otway Group|73594|5|Briefly described|p2, p4, p14|Cenomanian|Tithonian|Otway Basin.|||Casterton Formation, Crayfish Subgroup, Eumeralla Formation|Underlies Sherbrook Group||
14691|Outalpa Quartzite|23818|6|Mentioned|p33|||||||||
14691|Outalpa Quartzite|34537|6|Mentioned|p33|||||||||
14691|Outalpa Quartzite|38068|5|Briefly described|p67|||||||||
14730|Paaratte Formation|12781|6|Mentioned|p386|Late Cretaceous|Late Cretaceous|Otway Basin. Maximum thickness 1987m.||Sherbrook Group.||Overlies Belfast Mudstone and Flaxman Formation. Abuts Timboon Sandstone.||
14730|Paaratte Formation|12796|4|Described|p460, p456 Fig. 2|Campanian|Santonian|Of  Sherbrook Gp. Originally included members - Belfast Mdst Mbr, Nullawarre Greensand and Timboon Sand Mbr - which are now formations. Interfingers with and overlies Skull Creek Mdst. Geol. Prov: Otway Basin.||||||
14730|Paaratte Formation|22674|5|Briefly described|Fig.2 p719|Maastrichtian|Santonian|||||||
14730|Paaratte Formation|22875|3|Fully described|p44|Late Cretaceous|Late Cretaceous|Sherbrook Group.||||||14-APR-08
14730|Paaratte Formation|22944|5|Briefly described|Fig3|||||||||
14730|Paaratte Formation|23818|4|Described|p164|Late Cretaceous|Late Cretaceous|Overlain by Curdie Formation. Underlain by Belfast Mudstone. Max. thickness: 5 800 ft.||||||29-JAN-07
14730|Paaratte Formation|23830|6|Mentioned|Fig. 6|||Geological Province: Gambier Embayment, Otway Basin.||||||24-JAN-06
14730|Paaratte Formation|24056|5|Briefly described|p85|Late Cretaceous|Late Cretaceous|Of Sherbrook Group. Geological Province: Otway Basin.||||||14-APR-08
14730|Paaratte Formation|24314|5|Briefly described|p61 Fig.2||Santonian|Geological Province: Otway Basin. Max. Thickness 1987m. Of the Sherbrook Group.||||||30-NOV-04
14730|Paaratte Formation|24453|5|Briefly described|p809 Fig.2|Maastrichtian|Santonian|Of Sherbrook Group. Overlain by Tomboon Sandstone Member, overlies Belfast Mudstone and Nullawarre Greensand. Geological Province: Otway Basin.||||||07-FEB-11
14730|Paaratte Formation|24551|6|Mentioned|p245|||Of the Sherbrook Group.||||||14-APR-08
14730|Paaratte Formation|24562|5|Briefly described|p3, 8|Late Cretaceous|Late Cretaceous|Of the Sherbrook Group. Geological Province: Otway Basin.||||||14-APR-08
14730|Paaratte Formation|29697|6|Mentioned|Fig.11|||||||||
14730|Paaratte Formation|29856|5|Briefly described|p38|||||||||
14730|Paaratte Formation|30499|6|Mentioned|p92|||Stratigraphy.||||||14-APR-08
14730|Paaratte Formation|30576|5|Briefly described|Table 2|||||||||
14730|Paaratte Formation|30578|5|Briefly described|p7|||||||||
14730|Paaratte Formation|30580|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
14730|Paaratte Formation|30675|5|Briefly described|p253|||Lithology and radioactivity.||||||29-JAN-07
14730|Paaratte Formation|30754|6|Mentioned|p12|||Stratigraphic table.||||||14-APR-08
14730|Paaratte Formation|30905|6|Mentioned|Table 7.3|||||||||
14730|Paaratte Formation|30932|6|Mentioned|Map legend|Late Cretaceous|Late Cretaceous|Part of Wangerrip Group.||||||14-APR-08
14730|Paaratte Formation|31245|6|Mentioned|p77|||||||||
14730|Paaratte Formation|31372|6|Mentioned|p2|||See also p9.||||||29-JAN-07
14730|Paaratte Formation|31396|6|Mentioned|p1185|||||||||
14730|Paaratte Formation|31424|4|Described|p17|||Described from core.||||||
14730|Paaratte Formation|31534|6|Mentioned|p393|||See also Table 19-3.||||||29-JAN-07
14730|Paaratte Formation|31624|6|Mentioned|Table 5-1|||See also Table 5-2.||||||29-JAN-07
14730|Paaratte Formation|31625|6|Mentioned|Fig. 5.2|||||||||
14730|Paaratte Formation|31714|6|Mentioned|Fig. 8|||||||||
14730|Paaratte Formation|31920|4|Described|p51|||U.Cret. Unit of Sherbrook Group.||||||29-JAN-07
14730|Paaratte Formation|31922|6|Mentioned|p187|||||||||
14730|Paaratte Formation|32344|6|Mentioned|Fig.2|||||||||
14730|Paaratte Formation|32852|6|Mentioned|p10|||||||||
14730|Paaratte Formation|32894|6|Mentioned|p286|||U.Cret.||||||
14730|Paaratte Formation|32896|6|Mentioned|Encl.7.1.|||U.Cret.||||||
14730|Paaratte Formation|32898|6|Mentioned|Table 2-1|||||||||
14730|Paaratte Formation|32899|4|Described|p164|||See also pp165-175.||||||29-JAN-07
14730|Paaratte Formation|33155|6|Mentioned|p115|||||||||
14730|Paaratte Formation|33165|6|Mentioned|Chart|||Correlation chart only.||||||14-APR-08
14730|Paaratte Formation|33936|6|Mentioned|Fig.6|||||||||
14730|Paaratte Formation|33940|6|Mentioned|Fig.21-1|||Turonian - Maastrichtian||||||
14730|Paaratte Formation|34063|6|Mentioned|p3|||U.Cret. Table||||||
14730|Paaratte Formation|34308|6|Mentioned|Fig.85|||U.Cret. Sherbrook Group.||||||14-APR-08
14730|Paaratte Formation|34611|5|Briefly described|p164|||Upper Cretaceous||||||
14730|Paaratte Formation|34987|3|Fully described|p171|||||||||
14730|Paaratte Formation|35013|6|Mentioned|p393|||||||||
14730|Paaratte Formation|35066|6|Mentioned|p205|||||||||
14730|Paaratte Formation|35285|6|Mentioned|p414|||||||||
14730|Paaratte Formation|35722|6|Mentioned|p3|||Stratigraphy.||||||
14730|Paaratte Formation|36366|6|Mentioned|p3|||||||||
14730|Paaratte Formation|36913|6|Mentioned|p81|||||||||
14730|Paaratte Formation|38444|6|Mentioned|p302|||||||||
14730|Paaratte Formation|38625|6|Mentioned|Table 2|||||||||
14730|Paaratte Formation|40003|5|Briefly described|p43|||See also Fig.10||||||
14730|Paaratte Formation|40560|5|Briefly described|Fig.3|||||||||
14730|Paaratte Formation|40947|6|Mentioned|p4|||||||||
14730|Paaratte Formation|41016|5|Briefly described|p214|||||||||
14730|Paaratte Formation|41185|6|Mentioned|p177|||||||||
14730|Paaratte Formation|41269|5|Briefly described|p245|||||||||
14730|Paaratte Formation|41642|4|Described|p244|||||||||
14730|Paaratte Formation|41701|6|Mentioned|Map legend|Paleocene||Age spelt Palaeocene.||||||
14730|Paaratte Formation|41704|6|Mentioned|p100|||||||||
14730|Paaratte Formation|41714|6|Mentioned|p301|||||||||
14730|Paaratte Formation|41726|3|Fully described|p421|||See also p427.||||||29-JAN-07
14730|Paaratte Formation|41769|5|Briefly described|p16|||See also p17.||||||29-JAN-07
14730|Paaratte Formation|41868|4|Described|p533|||||||||
14730|Paaratte Formation|41936|6|Mentioned|p75|||||||||
14730|Paaratte Formation|42079|6|Mentioned|Fig.2 P264|||||||||
14730|Paaratte Formation|42318|6|Mentioned|p7|||||||||
14730|Paaratte Formation|42361|3|Fully described|p16|Maastrichtian|Turonian|Usage restricted to original concept of McQueen (1961).||||||
14730|Paaratte Formation|42524|5|Briefly described|Fig.3 P27|||||||||
14730|Paaratte Formation|42545|6|Mentioned|p19|||In the Otway Basin.||||||29-JAN-07
14730|Paaratte Formation|42555|6|Mentioned|p285|||||||||
14730|Paaratte Formation|42599|5|Briefly described|Fig.3 P614|||||||||
14730|Paaratte Formation|42827|4|Described|p244|||||||||
14730|Paaratte Formation|42863|5|Briefly described|Fig.14|||Variation on Victorian unit.||||||
14730|Paaratte Formation|43052|5|Briefly described|Table 2.1|||||||||
14730|Paaratte Formation|43171|5|Briefly described|5-8|||Of Sherbrook Formation. Age: 65-85 Ma||||||
14730|Paaratte Formation|43195|5|Briefly described|Map Legend||Late Cretaceous|See also commentary on back of map. Of Sherbrook Group.||||||
14730|Paaratte Formation|43208|5|Briefly described|map legend|Maastrichtian|Santonian|Of Sherbrook Group.||||||
14730|Paaratte Formation|43219|5|Briefly described|Fig.3,p6.|Maastrichtian|Santonian|Of Sherbrook Group.||||||29-JAN-07
14730|Paaratte Formation|43590|4|Described|p14|Maastrichtian|Santonian|||||||
14730|Paaratte Formation|43660|6|Mentioned|Fig.6,p15||Late Cretaceous|||||||
14730|Paaratte Formation|43733|6|Mentioned|Fig.2.11,p65||Late Cretaceous|||||||
14730|Paaratte Formation|43744|6|Mentioned|Fig.3,p3|||||||||
14730|Paaratte Formation|43783|6|Mentioned|Fig14, p11||Late Cretaceous|||||||
14730|Paaratte Formation|43784|6|Mentioned|Fig10, p12||Late Cretaceous|||||||
14730|Paaratte Formation|43814|6|Mentioned|Fig.3,p115|||||||||
14730|Paaratte Formation|43937|5|Briefly described|Map Legend|Santonian|Aptian|||||||
14730|Paaratte Formation|44133|4|Described|p147|Maastrichtian|Santonian|Of the Sherbrook Group. Geological Province: Otway Basin. Previously 'Paaratte Formation'. Thickness: 1836m. Underlies Timboon Sandstone and Dilwyn Formation, unconformably.||||||29-JAN-07
14730|Paaratte Formation|48581|2|Defined|p33|||See also p12,28,29,34,38,40. Fig.4,6,Pl.1,2. Underlies Wangerrip Gp; Overlies Belfast Mudstone. (J54-12/Port Campbell).||||||07-APR-09
14730|Paaratte Formation|48624|14|Not recorded|p5,7,Fig.2|||(J54-6/Benara).||||||
14730|Paaratte Formation|48625|14|Not recorded|p7|||(J54-6/Benara).||||||
14730|Paaratte Formation|48911|3|Fully described|p20|||||||||
14730|Paaratte Formation|48977|6|Mentioned|Fig.5|||||||||
14730|Paaratte Formation|49060|5|Briefly described|Fig.33|||||||||
14730|Paaratte Formation|61017|5|Briefly described|p5 Fig. 2|Campanian|Campanian|Of the Sherbrook Group. Geological Province: Otway Basin.||||||07-FEB-11
14730|Paaratte Formation|61182|3|Fully described|p18, p32, p84|Maastrichtian|Santonian|Of Sherbrook Gp. Incl:Timboon Sand and Skull Creek Mbrs.Conformable on Nullawarre Greensand, and Belfast Mudst.near coast.Unconformable below Pebble Point Fm.Thick: 962m. Geol.Prov: Otway Basin. Age from spore-pollen zones. older in South Australia. Prev.incl: Belfast Mudst, Nullawarre Greensand, Timboon Sand||||||20-SEP-18
14730|Paaratte Formation|61230|5|Briefly described|p319 Fig.2, p329, p341, pp344-345.    |Campanian|Santonian|Delta front to delta plain progradational depositional settings.||Unit in Sherbrook Group.||Overlies Belfast Mudstone (Formation). Is overlain by Timboon Formation.|Sandstone, mudstone; increasingly sandstone-dominated up-unit to coarse sandstone and conglomerate.|
14730|Paaratte Formation|61470|5|Briefly described|p28 Fig. 5|Campanian|Campanian|Of the Sherbrook Group. Overlies Skull Creek Mudstone (with which it also interfingers); underlies Timboon Sandstone. Geological Province: Otway Basin.||||||12-OCT-05
14730|Paaratte Formation|61547|6|Mentioned|p461 Fig.2, p462. |Maastrichtian|Santonian|||Unit in Sherbrook Group.||Overlies Belfast Mudstone. Is overlain by Pebble Point Formation.||
14730|Paaratte Formation|61622|5|Briefly described|p436 Fig. 2|Cretaceous|Cretaceous|Sherbrook Group. Geological Province: Otway Basin.||||||07-FEB-11
14730|Paaratte Formation|61623|6|Mentioned|p449 Fig. 4|Late Cretaceous|Late Cretaceous|Of Sherbrook Group. Geological Province: Otway Basin.||||||07-APR-09
14730|Paaratte Formation|61625|5|Briefly described|p475, p476 Fig. 1, p477, p480, p483|Late Creatceous|Late Cretaceous|Of Sherbrook Group. Geological Province: Otway Basin. Mediun to fine-grained sandstone with rare molluscs with bioturbated mudstones.||||||07-FEB-11
14730|Paaratte Formation|61626|5|Briefly described|p486, p486 Fig. 2|Late Cretaceous|Late Cretaceous|Of Sherbrook Group. Geological Province: Otway Basin.||||||07-APR-09
14730|Paaratte Formation|61627|5|Briefly described|p500 Fig. 2|Late Cretaceous|Late Cretaceous|Of Sherbrook Group. Geological Province: Otway Basin.||||||07-FEB-11
14730|Paaratte Formation|61628|5|Briefly described|p509 Fig. 3|Late Cretaceous|Late Cretaceous|Of Sherbrook Group. Geological Province: Otway Basin.||||||07-APR-09
14730|Paaratte Formation|63124|3|Fully described|p48 Fig. 5.1, p49 Fig. 5.2, p82|Late Cretaceous|Late Cretaceous|Past stratigraphy has included various nomenclatures for Skull Creek Member and Timboon Sand Member. Timboon now of formation status - as Timboon Sandstone; Skull Creek units are incorp.into Paaratte Formation. Max. thickness:1987m. Geol.Prov: Otway Basin||||||
14730|Paaratte Formation|63125|6|Mentioned|p121 Tb. 7.11|||Geological Province: Otway Basin.||||||14-APR-08
14730|Paaratte Formation|63129|5|Briefly described|p137|||Offshore, this unit is an interbedded shale-sand facies into which the Timboon Sandstone passes laterally. Geological Province: Otway Basin.||||||14-APR-08
14730|Paaratte Formation|63269|5|Briefly described|p605-606|Late Cretaceous|Late Cretaceous|Otway Basin. Details of oils and oil stains in named wells tabulated. Appears as Parratte Sandstone [!] on p606.||Sherbrook Group.||||
14730|Paaratte Formation|63431|5|Briefly described|p677 Fig. 2|Maastrictian|Santonian|Of the Sherbrook Group. Geological Province: Penola Trough/Otway Basin.||||||07-FEB-11
14730|Paaratte Formation|66245|5|Briefly described|p6 Fig.5, p22 Fig.25, p63 Fig.C5.|Maastrichtian|Santonian|||Unit in Sherbrook Group.||Overlies Belfast Mudstone. Is intercalated with Nullawarre Greensand. Is overlain by Timboon Sandstone.||
14730|Paaratte Formation|67061|6|Mentioned|p546 Fig.3.|Late Cretaceous|Late Cretaceous|||Unit in Sherbrook Group.||Is overlain by Timboon Sandstone.||15-MAR-12
14730|Paaratte Formation|67366|5|Briefly described|p103 Fig.2, p124.|Campanian|Campanian|Contains biodegraded gas.||Unit in Sherbrook Group.||Overlies Skull Creek Mudstone. Is overlain by Timboon Sandstone.|Shallow to nearshore marine sandstone and shale.|
14730|Paaratte Formation|67367|5|Briefly described|p131 Fig.2. |Campanian|Campanian|||Unit in Sherbrook Group.||||
14730|Paaratte Formation|69297|5|Briefly described|p79, p84, p98, p115|Maastrichtian|Campanian|Otway Basin. Contains good quality reservoir intervals.||Sherbrook Group||Overlies the Belfast Mudstone or the Skull Creek Mudstone. Faulted against or overlain by the Timboon Sandstone.|Siltstones.|
14730|Paaratte Formation|69651|5|Briefly described|p10, p27, p32-34|Late Cretaceous|Late Cretaceous|Campanian-Maastrichtian age. Contains good-quality reservoirs; intraformational mudstones may form seals. Has gas shows in tilted fault blocks.||Sherbrook Group.||Overlies Belfast Mudstone. Is interbedded with Nullawarre Greensand. Is overlain by Timboon Sandstone.||
14730|Paaratte Formation|70077|5|Briefly described|Nelson: Fig.2; p2. Regional: Fig.4; p8|Campanian|Santonian|See also Regional: p10-11. Otway Basin. Distal sandstone equivalents in the Nelson Sub-basin may be important petroleum reservoirs. Also contains intraformational mudstones with good sealing capacity.||Sherbrook Group.||Overlies Mount Salt Formation, Belfast or Skull Creek Mudstones. Is overlain by Timboon Sandstone.||
14730|Paaratte Formation|70078|5|Briefly described|Northern: Fig.2; p2. Regional: Fig.4|Campanian|Santonian|Otway Basin. Sandstones equivalent to this unit in the Sorell Basin are potential hydrocarbon sources. Similarly, equivalent rocks are potential intraformational seals.||Sherbrook Group.||Overlies Mount Salt Formation. Is overlain by Timboon Sandstone.||
14730|Paaratte Formation|70193|5|Briefly described|p283, p284, p285-288|Campanian|Campanian|Geological province: Otway Basin. X. australis dinocyst zone; formation varies in thickness from 160 to 339m.||Unit of the Sherbrook Supersequence||Underlain unconformably by Skull Creek Mudstone, overlain conformably by Timboon Sandstone.|Carbonaceous, interbedded and laminated fine-grained sandstone, siltstone and mudstone with thin beds of coarse sandstone and gravel.|30-MAY-19
14730|Paaratte Formation|70880|6|Mentioned|p77|Maastrichtian|Coniacian|Otway Basin. Hydrocarbon reservoir.||||||
14730|Paaratte Formation|70942|6|Mentioned|p118|||||||||
14730|Paaratte Formation|71266|6|Mentioned|p614 Fig.3|Late Cretaceous|Late Cretaceous|Otway Basin.||||||
14730|Paaratte Formation|71437|4|Described|Fig. 1 opp 154,  p155, p157-158|Maastrichtian|Coniacian|Paralic, deltaic, lagoonal and tidal flat environment.||Of Wangerrip Group.|Includes Belfast Mudstone, Nullawarre Greensand, Timboon Sand members.|Gradational, transitional or interfingering  with Timboon Sand Mmeber. Unconformably overlain by Pebble Point Formation.|Clay-silt shale, quartz sand, silty sand, minor glauconite, coal, and ankerite-siderite. Well-bedded and laminated.|
14730|Paaratte Formation|73357|5|Briefly described|p21-24, p31, p45, p47|Campanian|Santonian|Otway Basin. Skull Creek Mudstone/Paaratte Formation boundary is diachronous, and lithostratigraphic boundary with Timboon Sandstone can be uncertain. Correlated with Nelsoniella aceras Dinocyst Zone, Xenikoon australis Dinocyst Zone, nearshore to marginal marine depositional environments. Correlated to multiple biozones including Tricolpites apoxyexinus Spore-Pollen Zone in western regions. Upper part correlated with Isabelidinium pellucidum Dinocyst Zone, and Forcipites longus Spore-Pollen Zone at uppermost part.||Of Sherbrook Group.||Overlies Skull Creek Mudstone, underlies Timboon Sandstone.|Includes shales.|
14730|Paaratte Formation|73383|5|Briefly described|p3, p10 Tb.3.7, p22-23, p247-248, p258|Maastrichtian|Campanian|Otway Basin. Approximately equivalent to chemostratigraphic package S5-P7 containing high Th/Sc and Si/Al values, low Th/K and Sm/U values. Intervals are also assigned to chemostratigraphic package S5-P5 defined by high Fe and P values. Lithologies based on geochemistry using the ChemLith classification includes sandstones, calcareous and argillaceous sandstones, calcareous limestone; and using the Herron classification (1988) includes lith-arenite, Fe-sand and Fe-shale. See also vi, p11 Tb.3.9, p67, p119, p131-132, p140, p199-200, p258-260, p267, p322, p325.||Sherbrook Group||Overlies Skull Creek Mudstone, Nullawarre Greensand, underlies Timboon Sandstone|Predominantly sand lithologies, including quartz arenites, sublith-arenites and subarkose.|
14730|Paaratte Formation|73385|5|Briefly described|p5|Maastrichtian|Campanian|Otway Basin.||Sherbrook Group||Overlies Skull Creek Mudstone, Nullawarre Greensand, underlies Timboon Sandstone.|Shallow marine and nearshore sandstones.|
14730|Paaratte Formation|73386|4|Described|p4, p6, p10-11, Attachment A1|Maastrichtian|Santonian|Otway Basin. Diachronous unit deposited across the Otway Basin, extends from Tricolporites apoxyexinus Spore-Pollen Zone to Lower Forcipites longus Spore-Pollen Subzone. Changes facies from upper delta plain to upper delta front interbedded sandstones and shales onshore and nearshore, to lower delta front and prodelta siltstones and shales further offshore. Interfingers with Skull Creek Mudstone in Port Campbell and Tyrendarra embayments.||Sherbrook Group||Overlies and interfingers with Skull Creek Mudstone, overlies Nullawarre Greensand, Belfast Mudstone, underlies Timboon Sandstone|Interbedded fine to coarse grained sandstones with mudstone and occasional coals.|
14730|Paaratte Formation|73594|5|Briefly described|p4-5, p13|Maastrichtian|Campanian|Otway Basin.||Sherbrook Group||Overlies Skull Creek Mudstone, Nullawarre Greensand, underlies Timboon Sandstone|Shallow marine and nearshore sandstones.|
14744|Pacoota Sandstone|9199|5|Briefly described|Map legend|Ordovician|Cambrian|Contains the N'Dahla Member.  Fossiliferous sandstone and silty sandstone.  Geological Province: Amadeus Basin.||||||04-NOV-04
14744|Pacoota Sandstone|9814|5|Briefly described|Map Legend|Ordovician|Ordovician|Of the Larapinta Group. Fossiliferous sandstone, silty sandstone, siltstone.||||||
14744|Pacoota Sandstone|12891|6|Mentioned|p734|||Geological province: Amadeus Basin. See also the misspelt Pakoota Sandstone.||||||07-FEB-11
14744|Pacoota Sandstone|13995|5|Briefly described|p75-76, p81-82, p91, p95|Ordovician|Cambrian|Shergold et al. (1991). Amadeus Basin. Platform deposits associated with Delamerian Orogeny. Contains rostroconchs (named) in beds of Datsonian (latest Cambrian) age. The oldest known diverse fauna of pelecypods in the world occurs in Warendian (Tremadocian) beds of this unit: species listed. Contains microvertebrate remains.|||||Coarse siliciclastics.|
14744|Pacoota Sandstone|22560|5|Briefly described|p3|||||||||
14744|Pacoota Sandstone|22561|4|Described|p28|Neoproterozoic|Neoproterozoic|Horn Valley Siltstone overlies this unit.||||||22-NOV-06
14744|Pacoota Sandstone|22565|5|Briefly described|p71 & Table 1|||Thickness at Areyonga Creek measured from surface expression - 560m thick.  Approx. thickness measured from seismic data - 350m.||||||
14744|Pacoota Sandstone|22566|4|Described|p84|Early Devonian|Late Cambrian|Of the Larapinta Group.||||||22-NOV-06
14744|Pacoota Sandstone|22646|5|Briefly described|p 105|Ordovician|Cambrian|informal division - lower Pacoota Sandstone refered to p 104||||||
14744|Pacoota Sandstone|22650|4|Described|p 160|Ordovician|Cambrian|Of the Larapinta Group.||||||22-NOV-06
14744|Pacoota Sandstone|22651|5|Briefly described|p 174||Late Cambrian|A major sequence boundary lies at the base of the Pacoota Sandstone which overlies the Pertaoorrta Group.||||||
14744|Pacoota Sandstone|22655|5|Briefly described|p 253|||||||||
14744|Pacoota Sandstone|22656|4|Described|p 277|Early Ordovician|Late Cambrian|||||||
14744|Pacoota Sandstone|22657|4|Described|p 285|Early Ordovician|Late Cambrian|Subdivided into p1-4.||||||22-NOV-06
14744|Pacoota Sandstone|22758|4|Described|p303-307|||Informally divided into upper and lower Pacoota Sandstone. The upper Pacoota Sandstone is Early Arenig in Age. The Pacoota Sandstone contains oolitic ironstones in the Henbury and Lake Amadeus Regions.||||||06-FEB-08
14744|Pacoota Sandstone|22759|5|Briefly described|p317|||Age Cambro-Ordovician.||||||
14744|Pacoota Sandstone|22760|6|Mentioned|p338|||||||||
14744|Pacoota Sandstone|22762|5|Briefly described|p364|Early Ordovician|Late Cambrian|||||||
14744|Pacoota Sandstone|22763|6|Mentioned|p398|Early Ordovician|Cambrian|Of the Larapinta Group.||||||22-NOV-06
14744|Pacoota Sandstone|22804|5|Briefly described|p452|Early Ordovician|Late Cambrian|Of the Larapinta Group.||||||22-NOV-06
14744|Pacoota Sandstone|22805|4|Described|p463-471|Early Ordovician|Late Cambrian|Capable of sustaining economic hydrocarbon flows p468.||||||
14744|Pacoota Sandstone|22806|4|Described|p486 & Tab 3 @p488|||Age - Cambro-Ordovician p481.  Informally devided into subunits p1-4, p480.||||||22-NOV-06
14744|Pacoota Sandstone|22807|4|Described|p499 & p500-503|Early Ordovician|Late Cambrian|Of the Larapinta Group.  The Pacoota Sandstone has been divided into four subunits, from top to bottom p1-3 and p4;  see also p499.||||||22-NOV-06
14744|Pacoota Sandstone|22824|4|Described|p526-530|Early Ordovician|Late Cambrian|Of the Larapinta Group.  Age - late Payntonian to early Arenigian, this correlates to an age range of 508-480 Ma.  See p526.||||||22-NOV-06
14744|Pacoota Sandstone|22825|6|Mentioned|p543|Early Ordovician|Early Ordovician|||||||
14744|Pacoota Sandstone|22826|4|Described|p572|Ordovician|Late Cambrian|Of the Larapinta Group.||||||22-NOV-06
14744|Pacoota Sandstone|22828|6|Mentioned|p591|||||||||
14744|Pacoota Sandstone|23250|5|Briefly described|p1124  Fig.2||Late Cambrian|Correlate of Lake Frome Group.||||||
14744|Pacoota Sandstone|23282|6|Mentioned|p81|||Probably equivalent to Mount Chandler Sandstone in Officer Basin. In the Amadeus Basin.||||||22-NOV-06
14744|Pacoota Sandstone|23361|5|Briefly described|16 Fig.4|Cambrian|Cambrian|||||||
14744|Pacoota Sandstone|23373|6|Mentioned|p318||Early Ordovician|In the Amadeus Basin.||||||22-NOV-06
14744|Pacoota Sandstone|23818|6|Mentioned|p111|||Correlated with Mount Chandler Sandstone. Geological Province: Amadeus Basin.||||||
14744|Pacoota Sandstone|23858|5|Briefly described|p915|Ordovician|Cambrian|Geological Province: Amadeus Basin.||||||
14744|Pacoota Sandstone|24047|5|Briefly described|p60|Late Cambrian|Late Cambrian|Geological Province: Amadeus Basin.||||||
14744|Pacoota Sandstone|24063|5|Briefly described|p220|Ordovician|Cambrian|Geological Province: Amadeus Basin.||||||
14744|Pacoota Sandstone|24064|5|Briefly described|p229 Fig.7|Ordovician|Ordovician|Of Larapinta Group. Geological Province: Amadeus Basin.||||||
14744|Pacoota Sandstone|29591|5|Briefly described|Table 23|||||||||
14744|Pacoota Sandstone|29721|6|Mentioned|p46|||||||||
14744|Pacoota Sandstone|29972|6|Mentioned|Table 1|||||||||
14744|Pacoota Sandstone|30045|6|Mentioned|p344|||||||||
14744|Pacoota Sandstone|30238|4|Described|p68|||Cambrian - Ordovician age||||||
14744|Pacoota Sandstone|30258|6|Mentioned|Fig.2|||Ordovician age. Part of Larapinta Group||||||
14744|Pacoota Sandstone|30540|6|Mentioned|p61|||Possibly source rock||||||
14744|Pacoota Sandstone|30544|6|Mentioned|p49|||Ordovician age||||||
14744|Pacoota Sandstone|30598|6|Mentioned|p51|||||||||
14744|Pacoota Sandstone|30615|6|Mentioned|p177|||Ordovician Formation damage||||||
14744|Pacoota Sandstone|31566|6|Mentioned|p231|||See also Fig. 2||||||
14744|Pacoota Sandstone|31572|6|Mentioned|p21|||U.Camb. - L.Ord. Correlation chart 1||||||
14744|Pacoota Sandstone|31707|4|Described|p50|||Lithology||||||
14744|Pacoota Sandstone|32712|6|Mentioned|Table 1|||||||||
14744|Pacoota Sandstone|32715|6|Mentioned|p1177|||Oil||||||
14744|Pacoota Sandstone|33307|6|Mentioned|Fig.6|||||||||
14744|Pacoota Sandstone|33491|6|Mentioned|p55|||||||||
14744|Pacoota Sandstone|33738|6|Mentioned|p47|||||||||
14744|Pacoota Sandstone|33761|6|Mentioned|p146|||Ord. Of the Larapinta Group.||||||22-NOV-06
14744|Pacoota Sandstone|33971|6|Mentioned|p26|||Refers gas production.||||||
14744|Pacoota Sandstone|34111|5|Briefly described|Table 2|||See also pp15,18. Cambrian - Ordovician||||||22-NOV-06
14744|Pacoota Sandstone|34280|6|Mentioned|p10|||||||||
14744|Pacoota Sandstone|34287|6|Mentioned|p79|||||||||
14744|Pacoota Sandstone|34433|6|Mentioned|p17|||||||||
14744|Pacoota Sandstone|34442|5|Briefly described|Table 1|||Cambrian - Ordovician||||||
14744|Pacoota Sandstone|34579|4|Described|Table 2|||See also pp16,17. Cambrian - Ordovician.||||||22-NOV-06
14744|Pacoota Sandstone|34612|6|Mentioned|p111|||Correlation||||||
14744|Pacoota Sandstone|35102|6|Mentioned|Fig.2|||||||||
14744|Pacoota Sandstone|35628|6|Mentioned|Table 3|||||||||
14744|Pacoota Sandstone|35805|6|Mentioned|Fig.3|||||||||
14744|Pacoota Sandstone|36096|6|Mentioned|p219|||||||||
14744|Pacoota Sandstone|36128|6|Mentioned|p13|||||||||
14744|Pacoota Sandstone|36198|6|Mentioned|Fig.III.2|||||||||
14744|Pacoota Sandstone|36331|6|Mentioned|p6|||See also p30,36,44,53.||||||22-NOV-06
14744|Pacoota Sandstone|36643|6|Mentioned|p65|||||||||
14744|Pacoota Sandstone|36818|6|Mentioned|p203|||||||||
14744|Pacoota Sandstone|38329|6|Mentioned|p209|||||||||
14744|Pacoota Sandstone|38606|6|Mentioned|Map legend|Early Ordovician|Late Cambrian|Late Cambrian to Early Ordovician||||||
14744|Pacoota Sandstone|38885|6|Mentioned|Map legend|Early Ordovician|Late Cambrian|Late Cambrian - Early Ordovician||||||
14744|Pacoota Sandstone|39213|6|Mentioned|Fig.6|||Amadeus Basin Succession||||||
14744|Pacoota Sandstone|39214|6|Mentioned|p10|||||||||
14744|Pacoota Sandstone|39583|6|Mentioned|Map legend|Early Ordovician|Late Cambrian|Late Cambrian to Early Ordovician||||||
14744|Pacoota Sandstone|39931|6|Mentioned|Map legend|Early Ordovician|Late Cambrian|Late Cambrian to Early Ordovician||||||
14744|Pacoota Sandstone|40136|5|Briefly described|p36|||See also p23, p32||||||22-NOV-06
14744|Pacoota Sandstone|40740|3|Fully described|p50|||Mention p6.||||||22-NOV-06
14744|Pacoota Sandstone|40810|4|Described|p7|||||||||
14744|Pacoota Sandstone|40830|6|Mentioned|p12|||||||||
14744|Pacoota Sandstone|40852|6|Mentioned|p34|||||||||
14744|Pacoota Sandstone|40906|6|Mentioned|Fig.11|||||||||
14744|Pacoota Sandstone|41018|4|Described|Fig.3|||Mention Fig.2||||||
14744|Pacoota Sandstone|41039|4|Described|p3|||||||||
14744|Pacoota Sandstone|41115|6|Mentioned|Fig.2|||||||||
14744|Pacoota Sandstone|41123|6|Mentioned|p181|||||||||
14744|Pacoota Sandstone|41190|5|Briefly described|p267|||||||||
14744|Pacoota Sandstone|41203|5|Briefly described|p14|||||||||
14744|Pacoota Sandstone|41224|5|Briefly described|p433|||||||||
14744|Pacoota Sandstone|41270|6|Mentioned|p274|||See also p276||||||22-NOV-06
14744|Pacoota Sandstone|41385|6|Mentioned|Fig.2|||||||||
14744|Pacoota Sandstone|41409|6|Mentioned|p290|||||||||
14744|Pacoota Sandstone|41560|6|Mentioned|p551|||||||||
14744|Pacoota Sandstone|41621|5|Briefly described|Map legend|Early Ordovician|Late Cambrian|||||||
14744|Pacoota Sandstone|41639|6|Mentioned|p17|||||||||
14744|Pacoota Sandstone|41708|6|Mentioned|p198|||||||||
14744|Pacoota Sandstone|41711|6|Mentioned|p259|||||||||
14744|Pacoota Sandstone|41723|6|Mentioned|Map legend|Early Ordovician|Late Cambrian|||||||07-DEC-12
14744|Pacoota Sandstone|41820|3|Fully described|p8|||||||||
14744|Pacoota Sandstone|42037|5|Briefly described|Table 3 P79|||||||||
14744|Pacoota Sandstone|42049|5|Briefly described|p216|||||||||
14744|Pacoota Sandstone|42059|5|Briefly described|p130|||See also Fig.2||||||
14744|Pacoota Sandstone|42060|6|Mentioned|Fig.5 P140|||||||||
14744|Pacoota Sandstone|42082|4|Described|p322|||||||||
14744|Pacoota Sandstone|42354|2|Defined|p2-12|Bendigonian|Payntonian|Type section - Fig.2 p4.||||||22-NOV-06
14744|Pacoota Sandstone|42504|4|Described|p77|||||||||
14744|Pacoota Sandstone|42643|6|Mentioned|p32|||In the Amadeus Basin.||||||22-NOV-06
14744|Pacoota Sandstone|42940|6|Mentioned|Plate 5|||||||||
14744|Pacoota Sandstone|43035|6|Mentioned|p38|||||||||
14744|Pacoota Sandstone|43105|5|Briefly described|p8|||||||||
14744|Pacoota Sandstone|43225|5|Briefly described|Map Legend|Ordovician|Cambrian|Of Larapinta Group.||||||22-NOV-06
14744|Pacoota Sandstone|43230|6|Mentioned|p9||Ordovician|Reservoir target.||||||
14744|Pacoota Sandstone|43503|6|Mentioned|11-50|Bendigonian|Payntonian|||||||
14744|Pacoota Sandstone|43646|6|Mentioned|Fig.3,p554|Bendigonian|Payntonian|||||||
14744|Pacoota Sandstone|43647|6|Mentioned|p535|||||||||
14744|Pacoota Sandstone|43648|6|Mentioned|p491|||||||||
14744|Pacoota Sandstone|43649|5|Briefly described|p457|||||||||
14744|Pacoota Sandstone|43781|6|Mentioned|p4|||||||||
14744|Pacoota Sandstone|43803|6|Mentioned|Fig.5,p71|||||||||
14744|Pacoota Sandstone|43809|6|Mentioned|Fig.3,p215|||||||||
14744|Pacoota Sandstone|43817|5|Briefly described|p61-63|||||||||
14744|Pacoota Sandstone|43869|6|Mentioned|p10||Cambrian|||||||
14744|Pacoota Sandstone|43883|14|Not recorded|p11|||||||||
14744|Pacoota Sandstone|44133|5|Briefly described|p40, 43, 4 Fig. 7.2|Early Ordovician|Early Ordovician|Geological Province: Western Warburton Basin.||||||
14744|Pacoota Sandstone|44158|6|Mentioned|p33|||In the Amadeus Basin..||||||22-NOV-06
14744|Pacoota Sandstone|44395|14|Not recorded|p.8,10,12, Tb.2|||Camb-Ord.||||||
14744|Pacoota Sandstone|44396|5|Briefly described|map legend|||(Camb-Ord). Of Larapinta Group.||||||22-NOV-06
14744|Pacoota Sandstone|44402|5|Briefly described|map legend|Ordovician|Cambrian|Part of Larapinta Group. Camb-Ord.||||||02-DEC-04
14744|Pacoota Sandstone|44433|14|Not recorded|map legend|||Cambrian to Ordovician.||||||
14744|Pacoota Sandstone|44484|14|Not recorded|p.11,12,13,Tb.1,2|||Part Of Larapinta Group. (Camb-Ord).||||||
14744|Pacoota Sandstone|44485|14|Not recorded|map legend|Ordovician|Cambrian|Part of Larapinta Group. Camb-Ord. Defn on Tech.File F/53-13.||||||
14744|Pacoota Sandstone|44497|4|Described|p.10, Table 2|Ordovician|Cambrian|SF/53-13. Cambrian-Ord.||||||
14744|Pacoota Sandstone|44498|14|Not recorded|map legend|Ordovician|Cambrian|Part of Larapinta Group. Cambrian-Ord.||||||
14744|Pacoota Sandstone|44505|14|Not recorded|p.8,11, Table 1,2|Ordovician|Cambrian|Of Larapinta Group. Camb-Ord.||||||
14744|Pacoota Sandstone|44506|14|Not recorded|map legend|||Cambrian to Ordovician.||||||07-DEC-12
14744|Pacoota Sandstone|45036|6|Mentioned|p3|||||||||
14744|Pacoota Sandstone|45041|4|Described|p62|||See also pp63-68. U.Camb. - L.Ord.||||||22-NOV-06
14744|Pacoota Sandstone|45115|6|Mentioned|p7|||||||||
14744|Pacoota Sandstone|45118|6|Mentioned|p1,3|||||||||
14744|Pacoota Sandstone|45148|6|Mentioned|Fig.4|||In the Amadeus Basin.||||||22-NOV-06
14744|Pacoota Sandstone|45153|6|Mentioned|App.1-2|||||||||
14744|Pacoota Sandstone|45155|6|Mentioned|Fig.8|||||||||
14744|Pacoota Sandstone|45168|6|Mentioned|p6|||||||||
14744|Pacoota Sandstone|45170|6|Mentioned|p8|||||||||
14744|Pacoota Sandstone|46730|5|Briefly described|p7|Ordovician|Cambrian|Underlain by Pertaoorrta Group. Geological Province: Amadeus Basin||||||22-NOV-06
14744|Pacoota Sandstone|46826|5|Briefly described|p345|||||||||
14744|Pacoota Sandstone|46928|6|Mentioned|Table 1|||||||||
14744|Pacoota Sandstone|47050|6|Mentioned|p240|||||||||
14744|Pacoota Sandstone|48639|14|Not recorded|pages not known|||||||||
14744|Pacoota Sandstone|48838|2|Defined|p.19, Tb.1|||||||||
14744|Pacoota Sandstone|48862|14|Not recorded|p.8-18,23-25,40,41|||Basal unit of Larapinta Group. (F52-15). Pl.3,8-11.||||||22-NOV-06
14744|Pacoota Sandstone|48863|2|Defined|p.24,25|Early Ordovician|Late Cambrian|Tb.1. opp.p.7,9,14,20,29,30,36,37,39-41, Pl.3,4,9,10,11,13,15,16. Upper Cambrian-Lower Ordovician. (G52-4,G53-1).||||||
14744|Pacoota Sandstone|48864|14|Not recorded|p.10(Tb),31-33||Ordovician|||||||
14744|Pacoota Sandstone|48865|14|Not recorded|Fig.4,p.23,24|||(G52-4,F53-13)(Larapinta Gp.).||||||
14744|Pacoota Sandstone|48890|4|Described|p.44|Ordovician|Cambrian|See also Tables, Figs and Plates. Part of Larapinta Group. Camb-Ord.||||||22-NOV-06
14744|Pacoota Sandstone|48963|6|Mentioned|p5|||Fig.3||||||
14744|Pacoota Sandstone|50089|5|Briefly described|p430 Fig. 5|Ordovician|Ordovician|Geological Province: Amadeus Basin.||||||
14744|Pacoota Sandstone|50097|5|Briefly described|p44|Bendigonian|Lancefieldian|Geological Province: Amadeus Basin.||||||07-FEB-11
14744|Pacoota Sandstone|50098|5|Briefly described|p1|Ordovician||Of the Larapinta Group. Geological Province: Amadeus Basin.||||||
14744|Pacoota Sandstone|50246|5|Briefly described|p20 Fig. 2|Ordovician|Cambrian|Sandstone, siltstone - fossiliferous.||||||07-FEB-11
14744|Pacoota Sandstone|60287|5|Briefly described|p384|Ordovician|Cambrian|Thickness: 200 m.||||||
14744|Pacoota Sandstone|60547|5|Briefly described|Map Legend|Ordovician|Cambrian|Fossiliferous sandstone and silty sandstone. Of the Larapinta Group. Geological Province: Amadeus Basin.||||||03-JUN-05
14744|Pacoota Sandstone|60674|5|Briefly described|Map legend|Ordovician|Cambrian|Of the Larapinta Group. Medium cross-bedded quartz sandstone; minor coarse sandstone and pebbly beds. Geological Province: Amadeus Basin.||||||
14744|Pacoota Sandstone|61306|5|Briefly described|p14, p40|||High-yielding aquifer rocks. Geological Province: northern Amadeus Basin.||||||22-NOV-06
14744|Pacoota Sandstone|61309|5|Briefly described|p16 Fig. 4|||Geological Province: Amadeus Basin.||||||06-FEB-08
14744|Pacoota Sandstone|61385|5|Briefly described|Map legend|Ordovician|Cambrian|Sandstone, conglomeratic sandstone; marine fossils.   Geological Province: Ngalia Basin [?check map].||||||20-OCT-10
14744|Pacoota Sandstone|61387|5|Briefly described|Map legend|Ordovician|Ordovician|Of the Larapinta Group. Sandstone; marine fossils. Geological Province: Amadeus Basin.||||||04-OCT-05
14744|Pacoota Sandstone|61518|5|Briefly described|Map Legend|Ordovician|Cambrian|Of the Larapinta Group. Medium grained cross bedded quartz sandstone; minor coarse grained sandstone and pebbly beds. Geological Province: Amadeus Basin.||||||
14744|Pacoota Sandstone|61519|5|Briefly described|Map Legend|Ordovician|Ordovician|Of the Larapinta Group. Sandstone; marine fossils. Geological Province: Amadeus Basin.||||||14-FEB-06
14744|Pacoota Sandstone|62359|5|Briefly described|p542, p546|Ordovician|Ordovician|Overlain by Horn Valley Siltstone. Forms the reservoir for main hydrocarbon-producing system of the basin.  Geological Province: Amadeus Basin. See also p546-547 Figs. 6 and 7.||||||
14744|Pacoota Sandstone|62376|5|Briefly described|p18|Early Ordovician|Late Cambrian|Of the Larapinta Group. Geological Province: Amadeus Basin.||||||09-FEB-10
14744|Pacoota Sandstone|62379|5|Briefly described|p7 Fig. 2|Ordovician|Late Cambrian|Of the Larapinta Group. Geological Province: Amadeus Basin.||||||
14744|Pacoota Sandstone|62595|5|Briefly described|p9, p29 Fig.6, p30 Fig.8.|Ordovician|Cambrian|Widespread unit; the principal hydrocarbon reservoir in the Amadeus Basin. Contains 600-500 Ma detrital zircons with no apparent Central Australian source.|||||Mainly marine siliciclastics: fossiliferous sandstone and siltstone.|
14744|Pacoota Sandstone|62794|5|Briefly described|p288, p289 Fig.2, p290-291|Early Ordovician|Late Cambrian|Basal unit of Larapinta Group. Resistant quartzose sandstone, siltstone. Overlain by Horn Valley Siltstone. The boundary between these units has been revised several times (Prichard & Quinlan 1962; Wells et al.1970; Huckaba 1970; Gorter 1984,1991).||||||
14744|Pacoota Sandstone|62982|5|Briefly described|p7|Early Ordovician|Late Cambrian|Of the Larapinta Group. Thick shallow marine deposits with fluvial interludes. Overlain by Horn Valley Siltstone. Geological Province: Amadeus Basin. Main reservoir of Larapinta Group is in upper section of this unit.||||||05-FEB-08
14744|Pacoota Sandstone|63121|6|Mentioned|p231|||||||||
14744|Pacoota Sandstone|63562|4|Described|p338 fig 3, p341, p352 fig 10|Early Ordovician|Late Cambrian|See also p353 fig 11, p346-9. Of Amadeus Basin. Marine/locally fluvial, widespread siliciclastic unit. Zircon ages very mixed. Principal hydrocarbon reservoir in the Basin.||Larapinta Group||Overlies Goyder Formation. Is overlain by Horn Valley Siltstone. Correlated with Tomahawk Formation.|Medium-grained quartz sandstone.|
14744|Pacoota Sandstone|64068|6|Mentioned|p71, 72, 73, 75|||Amadeus Basin. Basal part may correlate with Chatsworth Limestone. Correlated with Ninmaroo Formation, Tomahawk Formation, Kelly Creek Formation, Georgina Basin.||||||
14744|Pacoota Sandstone|64334|5|Briefly described|p39-43, 45-46|Ordovician|Cambrian|Amadeus Basin. Is notably cyclic on several scales, shallowing-upward. Reservoir rock.||Larapinta Group.||Unconformably overlies Pertaoorrta Group. Is overlain by Horn Valley Siltstone.||
14744|Pacoota Sandstone|64778|6|Mentioned|p13|Ordovician|Ordovician|Amadeus Basin.||||||
14744|Pacoota Sandstone|64809|5|Briefly described|p2, p3 Fig.2, p6 Fig.4, p11 Fig.10.|Early Ordovician|Late Cambrian|See also p13 Fig.13. Marine transgression.||Of the Larapinta Group||||
14744|Pacoota Sandstone|65233|4|Described|p3 Fig. 2, p9-10|Early Ordovician|Late Cambrian|Basal unit of Larapinta Group. Gradational with upper Goyder Fm below. Max. thickness: 800m. Geological province: Amadeus Basin. An important oil reservoir in mainly shallow marine deposits - further lithological details included.||||||07-FEB-11
14744|Pacoota Sandstone|65342|6|Mentioned|p4.|||Amadeus Basin. Max. thickness at least 384 m.||||Overlies Goyder Formation. Is overlain by Horn Valley Siltstone.||
14744|Pacoota Sandstone|65489|5|Briefly described|p125|Ordovician|Cambrian|Amadeus Basin. Hosts Mereenie oil field and the Palm Valley and West Walker gas fields.||Unit in Larapinta Group.||Overlies Goyder Formation (Pertaoorrta Group). Is overlain by Horn Valley Siltstone.||
14744|Pacoota Sandstone|66589|6|Mentioned|p178|Early Ordovician|Early Ordovician|Case studies cited; not visited in the field by the authors of this study.||||||
14744|Pacoota Sandstone|67326|4|Described|p2-6, p12-13, Appx.2|Early Ordovician|Late Cambrian|Amadeus Basin. The lower part of this unit was intersected by stratigraphic drillhole LA05DD01. Up to 800m thick; thins to the S. Mainly shallow-marine deposits. Unmetamorphosed. Cored section photograph. Contains viable reservoir-quality sandstone. Cu sulfides present in basal part. Composite log.||Larapinta Group.||Overlies Goyder Formation, and Petermann Sandstone ?disconformably. Is overlain by Horn Valley Siltstone.|Off-white to pink, occasionally red-yellow, cross-bedded, locally bioturbated and strongly limonitic, quartzose sandstone; minor metasedimentary, acid volcanic and kaolinitic clasts.|
14744|Pacoota Sandstone|67565|5|Briefly described|p40, p41, p50, p52.|Early Ordovician|Late Cambrian|Shallow marine environment. Forms prominent peaks and ridges. Is an important aquifer and oil and gas reservoir; it is the reservoir rock at the Mereenie oil/gas field. Up to 640 m thick. Hosts a significant manganese occurrence at the Wangatinya Prospect. An important aquifer.||||Conformably overlies Cleland Sandstone and Goyder Formation. Is overlain conformably by Horn Valley Siltstone.|Mainly a medium-grained, cross-bedded quartz sandstone, with minor coarse sandstone and pebbly beds; local prominent glauconitic bed.|
14744|Pacoota Sandstone|67856|6|Mentioned|p338 fig 4-30|Early Ordovician|Late Cambrian|||Of Larapinta Group.||||
14744|Pacoota Sandstone|68297|5|Briefly described|p177|Bendigonian|Bendigonian|Amadeus Basin. Includes disarticulated vertebrate fossils.||||||
14744|Pacoota Sandstone|68316|6|Mentioned|pp778-780, pp782-784|Early Ordovician|Early Ordovician|Amadeus Basin.|< c. 490 Ma, detrital zircon|||||
14744|Pacoota Sandstone|68323|5|Briefly described|p1-6, p8-10, p12-13, p15|Early Ordovician|Late Cambrian|Mineralogy detailed: dominated by quartz and kaolinite. The mineralogy is uniform across the logged boundary with the underlying unit.||Larapinta Group.||Overlies Petermann Sandstone, probably conformably.|Largely quartzose; minor metasedimentary, acid volcanic and kaolinitic clasts.|
14744|Pacoota 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
14744|Pacoota Sandstone|69437|5|Briefly described|p22:10, 15|Early Ordovician|Furongian|Amadeus Basin. Hosts the Wangatinya manganese prospect; currently uneconomic. Has considerable unconventional petroleum potential: tight gas.||||Overlies Goyder Formation. Is overlain by Horn Valley Siltstone.||12-JUL-16
14744|Pacoota Sandstone|69438|3|Fully described|p23:2-3,7-8,30,32-34,38,46,53-57,59-61|Early Ordovician|Late Cambrian|Pritchard and Quinlan (1962). Best exposed in prominent strike ridges and high escarpments in the MacDonnell, Idirriki and James Ranges and Johnny Creek Anticline, Amadeus Basin. 700-800m thick. Informally subdivided into four sequences (see Lithology), with a diverse fossil fauna at a number of levels. Sediment was sourced from the west and the east. Mapped (Wells et al., 1967) as including rocks subsequently assigned to N'Dahla Member (of Parke Siltstone) by Young et al. (1987). Hosts the Wangatinya manganese mineralisation. Contains oolitic ironstone beds with little economic significance. One of the main hydrocarbon reservoirs for the Basin, sealed by thick shales of the Horn Valley Siltstone.||Larapinta Group.||Overlies Cleland Sandstone conformably and Goyder Formation unconformably. Is overlain by N'Dahla Member unconformably and Horn Valley Siltstone probably unconformably.|Deeply incised, coarse-grained channel sandstone; strongly bioturbated sandstones with well-developed Skolithos ichnofacies; sandstones, glauconitic shale with dolostone layers; shales interbedded with sandstones rich in ichnofossils.|12-JUL-16
14744|Pacoota Sandstone|69439|5|Briefly described|p24:10|Ordovician|Ordovician|Amadeus Basin. Mentioned as having a similar fossil assemblage to the Bloodwood Formation (Ngalia Basin) which was nevertheless dated as Cambrian. Possible correlative of Djagamara Formation.||||||12-JUL-16
14744|Pacoota Sandstone|69443|6|Mentioned|p28:26-27|||Amadeus Basin.||||Correlated with Cockroach and Toko Groups.||12-JUL-16
14744|Pacoota Sandstone|69444|6|Mentioned|p29:2 Fig.29.3|||Amadeus Basin. Detrital zircon probability distribution diagram.||||||12-JUL-16
14744|Pacoota Sandstone|69449|5|Briefly described|p34:2 Fig.34.2; 34:4|Ordovician|Cambrian|Eastern Amadeus Basin.||Larapinta Group.||Probable correlative of Innamincka Formation.||12-JUL-16
14744|Pacoota Sandstone|69458|6|Mentioned|p42:33 Fig.42.37|||Amadeus Basin. Forms steeply-dipping strata in west MacDonnell Ranges with bevelled crests, interpreted as a preservation of an earlier upland surface.||||||12-JUL-16
14744|Pacoota Sandstone|69673|4|Described|p66, p87, p92, p93, p96,  p103, p149,|Ordovician|Cambrian|Deposited in shallow marine and paralic environments. 700-800m thick.||Larapinta Group||Unconformably overlies upper Goyder Formation, conformably overlain by Horn Valley Siltstone|Strongly bioturbated sandstones, sandstones overlain by glauconitic shale and dolostones. Black shales and siltstone interbeds.|
14744|Pacoota Sandstone|70094|6|Mentioned|p80|||Detrital zircons from this and other units were analysed to establish similar provenances for Harts Range Group, Amadeus and Georgina Basins.||||||
14744|Pacoota Sandstone|70749|6|Mentioned|p52, p54|||Amadeus Basin.||Larapinta Group.||||
14744|Pacoota Sandstone|71114|6|Mentioned|p170 fig 1b, p172-6. ||Furongian|Across entire Amadeus Basin. Downhole logs of petroleum wells Alice 1 and East Mereenie 4.||||Shown as overlying Goyder Formation.||14-FEB-18
14744|Pacoota Sandstone|71146|5|Briefly described|p6|Early Ordovician|Cambrian|Amadeus Basin.||Larapinta Group||Unconformably overlies the Pertaoorrta Group. Overlain by the Horn Valley Siltstone.|Sandstone.|
14744|Pacoota Sandstone|71171|6|Mentioned|p2|||Amadeus Basin.||||||
14744|Pacoota Sandstone|71279|5|Briefly described|p353, p355 Fig.2, p359, p366, p382 Tb.1|Early Ordovician|Late Cambrian|Amadeus Basin. Modelled magnetic properties.|<510 Ma (maximum depositional age).|Larapinta Group.|||Quartzite.|27-OCT-17
14744|Pacoota Sandstone|71283|6|Mentioned|p472, p478|Early Ordovician|Early Ordovician|Amadeus Basin. Trilobite species mentioned.||||||
14744|Pacoota Sandstone|71342|6|Mentioned|Ch9 p3, Ch9 p7, Ch9 p9, Ch9 p11, Ch9 p21|Palaeozoic|Palaeozoic|||||||
14744|Pacoota Sandstone|71800|5|Briefly described|p26-p27|Early Ordovician|Late Cambrian|Amadeus Basin.||||Unconformably overlies the Goyder Formation. Overlain by the Horn Valley Siltstone.|Sandstone and quartz sandstone.|
14744|Pacoota Sandstone|71898|5|Briefly described|p17|||Amadeus Basin.||Larapinta Group||Unconformably overlies the Goyder Formation. Conformably to unconformably overlain by the Horn Valley Siltstone.||19-NOV-18
14744|Pacoota Sandstone|72358|5|Briefly described|p118-119,121-126|Furongian|Furongian|Of Amadeus Basin. Contact with underlying Goyder Formation is brecciated and deformed, associated with anticlinal structural architecture of Waterhouse Range (Austin et al., 2017). This contact is described as a 2nd-order regressive sequence boundary in this study, marking a disconformity and erosional surface.||||Underlain by Goyder Formation.||10-JAN-20
14744|Pacoota Sandstone|72360|5|Briefly described|Map legend|Ordovician|Cambrian|Of Amadeus Basin.||Unit of Larapinta Group.|||Sandstone; marine fossils.|09-SEP-19
14744|Pacoota Sandstone|72369|4|Described|iii,p3-4,26-29|||Of Amadeus Basin. Outcrops extensively across the Amadeus Basin, and most well exposed as prominent strike ridges in the MacDonnell, Idirriki and James ranges, and in the Johnnys Creek Anticline. LA-ICP-MS U-Pb detrital zircon dating of sample HB15VJN345 (quartz arenite) yielded an interpreted maximum depositional age of 522+\-5 Ma (youngest concordant zircon), but does not further constrained the depositional age of the Pacoota Sandstone, as it pre-dates the c. 508-480 Ma age provided by fossils (see Shergold et al 1991), and the c. 488-486 Ma MDA provided by Maidment (2005). Contains detrital zircons sourced from Aileron and Warumpi provinces (c. 2000-1430 Ma age spectrum). Detrital zircons between c. 1255-850 Ma and c. 750-520 Ma are interpreted to have been sourced distally from east Gondwana as there are no known proximal Neoproterozoic-Cambrian sources to the Amadeus Basin. Diverse zircon age spectra and large proportion of rounded zircon grains, indicate at least partial derivation from intra-basinal recycling from older lithostratigraphic units.||Unit of Larapinta Group.||Unconformably overlain by Horn Valley Siltstone. Basal unit of Larapinta Group. Unconformably overlies the Goyder Formation.|Variably fine- to coarse-grained quartz sandstone.|18-DEC-19
14744|Pacoota Sandstone|72516|6|Mentioned|p94|Ordovician|Cambrian|Amadeus Basin.||||Equivalent to the Tomahawk Formation.||09-JUN-21
14744|Pacoota Sandstone|73085|4|Described|piii, p1, p3-8|early Ordovician|late Cambrian|Amadeus Basin. 62.5 m thick in drillhole LA05DD01. Basal contact with Petermann Sandstone is sharp.||Larapinta Group||Underlain by Pertermann Sandstone and Goyder Formation (Pertaoorrta Group and equivalents). Overlain by Horn Valley Siltstone.|White to brown, medium- to coarse-grained sandstone with occasional fine-grained, thinly laminated beds. Bedding and lamina planes are defined by red or orange Fe-oxide minerals. Cross-bedding was also observed in a short interval of core.|
14744|Pacoota Sandstone|73279|5|Briefly described|p3, p10|Ordovician[?]|Cambrian|Amadeus Basin. Lowermost part of the Larapinta Group. Detrital zircons analysed for Hf isotopic composition [see article].||Larapinta Group|||Includes sandstone.|
14744|Pacoota Sandstone|73346|6|Mentioned|p18|Early Ordovician|Furongian|Amadeus Basin. Includes the arandaspid Porophoraspis sp.||||||
14771|Padthaway Formation|10010|5|Briefly described|p14-15 Fig. 5e|Quaternary|Quaternary|Geological Province: Murray Basin.||||||13-AUG-07
14771|Padthaway Formation|29697|6|Mentioned|p23|||||||||
14771|Padthaway Formation|29892|6|Mentioned|p77|||||||||
14771|Padthaway Formation|33798|6|Mentioned|Fig.2|||||||||
14771|Padthaway Formation|38932|5|Briefly described|p99|||See also Fig.4||||||
14771|Padthaway Formation|42129|6|Mentioned|p254|||See also Fig.6||||||
14771|Padthaway Formation|42601|6|Mentioned|Fig.2 p15|||||||||
14771|Padthaway Formation|42966|3|Fully described|p227|||||||||
14771|Padthaway Formation|43053|5|Briefly described|Map Legend|Pleistocene|Pleistocene|Silt, dolomite and sand of lagoons and swamps.||||||25-MAY-05
14771|Padthaway Formation|43195|5|Briefly described|Map Legend|Late Pleistocene|Early Pleistocene|see also commentary on back of map.||||||
14771|Padthaway Formation|43258|5|Briefly described|Map Legend||Pleistocene|||||||
14771|Padthaway Formation|43298|5|Briefly described|Map Legend||Pleistocene|||||||
14771|Padthaway Formation|44133|5|Briefly described|p221 Fig. 11.3|Pleistocene|Pleistocene|Lagoonal and lacustrine facies.||||||
14771|Padthaway Formation|49038|5|Briefly described|p33|||||||||
14771|Padthaway Formation|50154|2|Defined|p21 Fig. 3.3, p26, p140|Recent|Pleistocene|Age: oldest dunes min. 0.69 Ma. Formation formed in the swales between dunes of the Bridgewater Formation. Consists of unconsolidated clay, sandy clay, calcareous clay, minor quartz sand and shell detritus.||||||23-MAY-13
14771|Padthaway Formation|50156|5|Briefly described|Map Legend|Pleistocene|Miocene|Lacustrine: lagoonal, swamp and locally colluvial deposits forming low-lying wetlands between stranded beach ridges: sand, silt, sandy clay, peat, marl, freshwater limestone; unconsolidated.||||||
14771|Padthaway Formation|50157|5|Briefly described|Map Legend|Recent|Pleistocene|Lacustrine: lagoonal, swamp and locally colluvial deposits forming low-lying wetlands between stranded beach ridges: sand, silt, sandy clay, peat, marl, freshwater limestone; unconsolidated.||||||
14771|Padthaway Formation|50158|5|Briefly described|Map Legend|Recent|Pleistocene|Lacustrine: lagoonal, swamp and locally colluvial deposits forming low-lying wetlands between stranded beach ridges: sand, silt, sandy clay, peat, marl, freshwater limestone; unconsolidated.||||||
14771|Padthaway Formation|50159|5|Briefly described|Map Legend|Recent|Pleistocene|Lacustrine: lagoonal, swamp and locally colluvial deposits forming low-lying wetlands between stranded beach ridges: sand, silt, sandy clay, peat, marl, freshwater limestone; unconsolidated.||||||24-JUN-04
14771|Padthaway Formation|50160|5|Briefly described|Map Legend|Recent|Pleistocene|||||||16-JUN-04
14771|Padthaway Formation|50161|5|Briefly described|Map Legend|Recent|Pleistocene|Lacustrine: lagoonal, swamp and locally colluvial deposits forming low-lying wetlands between stranded beach ridges: sand, silt, sandy clay, peat, marl, freshwater limestone; unconsolidated.||||||
14771|Padthaway Formation|50162|5|Briefly described|Map Legend|Recent|Pleistocene|Lacustrine: lagoonal, swamp and locally colluvial deposits forming low-lying wetlands between stranded beach ridges: sand, silt, sandy clay, peat, marl, freshwater limestone; unconsolidated.||||||
14771|Padthaway Formation|50163|5|Briefly described|Map Legend|Recent|Pleistocene|Lacustrine: lagoonal, swamp and locally colluvial deposits forming low-lying wetlands between stranded beach ridges: sand, silt, sandy clay, peat, marl, freshwater limestone; unconsolidated.||||||
14771|Padthaway Formation|60953|5|Briefly described|Map Legend|Pleistocene|Pleistocene|Silt, dolomite and sand of lagoons and swamps.||||||
14771|Padthaway Formation|61108|5|Briefly described|map legend|Pleistocene|Pleistocene|Silt, dolomite and sand of lagoons and swamps.||||||
14771|Padthaway Formation|61155|5|Briefly described|p6|Pleistocene|Pleistocene|Inter-ridge estuarine/lacustrine/lagoonal sequences. Geological Province: Otway and Murray Basins/coastal margins.||||||
14771|Padthaway Formation|63124|6|Mentioned|p93|||Geological Province: Gambier Basin.||||||
14771|Padthaway Formation|65376|5|Briefly described|p9 Fig.1.2. |Pleistocene|Pleistocene||||||Silt, dolomite and sand of lagoons and swamps.|
14771|Padthaway Formation|66002|5|Briefly described|p13 Tb.9|Neogene|Neogene|Defined by Harris 1973.||||||
14771|Padthaway Formation|68116|5|Briefly described|Appendix, Maps 29, 38, 47.|Pleistocene|Pleistocene||||||Lagoonal, swamp and locally colluvial deposits forming low-lying wetlands between stranded beach ridges: sand, silt, sandy clay, peat, marl, freshwater limestone; unconsolidated.|
14771|Padthaway Formation|68131|5|Briefly described|p2 Fig.1|Pleistocene|Pleistocene|Lagoon and swamp sediments.|||||Silt, dolomite and sand.|
14779|Paisley Pedoderm|31532|2|Defined|Table 1|Cenozoic|Cenozoic|||||||19-NOV-08
14779|Paisley Pedoderm|38605|6|Mentioned|p30|||||||||
14804|Palmer Granite|22634|6|Mentioned|p502|||||||||
14804|Palmer Granite|22643|6|Mentioned|p197|||||||||
14804|Palmer Granite|22726|6|Mentioned|p233|Late Cambrian|Neoproterozoic|||||||
14804|Palmer Granite|22945|6|Mentioned|p8|||Age - Cambro-Ordovician.  Mentioned under - Area C geology.||||||
14804|Palmer Granite|23023|6|Mentioned|Fig1p1798,1799|Arenig|Middle Cambrian|Age: 479 (+/-)15: Rb-Sr on total rocks and minerals; 503 (+/-) 33: Rb-Sr on total rocks only.||||||
14804|Palmer Granite|23818|5|Briefly described|p106|Ordovician|Ordovician|Age: 490 Ma.||||||
14804|Palmer Granite|23869|5|Briefly described|p15 Fig. 3|Cambrian|Cambrian|||||||
14804|Palmer Granite|30329|6|Mentioned|p30|||On table p30||||||16-MAR-22
14804|Palmer Granite|30398|6|Mentioned|p259|||||||||
14804|Palmer Granite|31321|6|Mentioned|p16|||Mineral deposits||||||
14804|Palmer Granite|32432|5|Briefly described|Table 1|||||||||
14804|Palmer Granite|32457|4|Described|p100|||||||||
14804|Palmer Granite|33471|6|Mentioned|p560|||||||||
14804|Palmer Granite|33845|6|Mentioned|p436|||Absolute age||||||
14804|Palmer Granite|34536|6|Mentioned|Map legend|Early Ordovician|Late Cambrian|Upper Cambrian - Lower Ordovician||||||
14804|Palmer Granite|34612|6|Mentioned|p106|||490my. Lower Ordovician||||||
14804|Palmer Granite|35357|6|Mentioned|p23|||||||||
14804|Palmer Granite|35358|3|Fully described|p18|||||||||
14804|Palmer Granite|36833|6|Mentioned|p23|||||||||
14804|Palmer Granite|37843|4|Described|p67|||||||||
14804|Palmer Granite|38068|5|Briefly described|p69|||||||||
14804|Palmer Granite|39331|6|Mentioned|Fig.0-3|||||||||
14804|Palmer Granite|39880|6|Mentioned|p351|||||||||
14804|Palmer Granite|40501|6|Mentioned|p118|||||||||
14804|Palmer Granite|42271|5|Briefly described|p384|||||||||
14804|Palmer Granite|42274|6|Mentioned|p458|||||||||
14804|Palmer Granite|42275|6|Mentioned|p469|||||||||
14804|Palmer Granite|42499|5|Briefly described|Map legend|Ordovician|Late Cambrian|||||||
14804|Palmer Granite|42884|5|Briefly described|Fig.1 P11|||||||||
14804|Palmer Granite|42971|5|Briefly described|p153|||||||||
14804|Palmer Granite|43190|6|Mentioned|Fig.1,p28.|||||||||
14804|Palmer Granite|43781|6|Mentioned|p3|||K/Ar Age: 504+/-33 Ma, 479+/-15 Ma||||||
14804|Palmer Granite|44133|5|Briefly described|p51 Fig. 7.18, 56 Table 7.3|Cambrian|Cambrian|Weakly lineated granite. I-Type. Age: 479 +/- 15Ma.||||||
14804|Palmer Granite|45087|5|Briefly described|p12|||Chemical analyses||||||
14804|Palmer Granite|61307|6|Mentioned|p12|||||||||
14804|Palmer Granite|67536|5|Briefly described|Map Legend|Tremodocian|Ediacaran|Kanmantoo Province; basement to Murray Basin.|ca. 564 +/- 57 Ma - 486 +/- 6 Ma||||Pre/syn-Delamerian felsic intrusive rocks.|
14804|Palmer Granite|70382|6|Mentioned|p34|Early Ordovician|Cambrian|Felsic intrusive magmatic phase during the late stages of, and immediately post-dating Cambrian Delamerian Orogeny (Foden et al., 2002, 2006; Preiss 1995).|~510-480 Ma||||A-type granite.|
14818|Pandurra Formation|22613|5|Briefly described|p14|Mesoproterozoic|Mesoproterozoic|Gawler Craton||||||
14818|Pandurra Formation|22629|6|Mentioned|fig1p146,158|Calymmian|Calymmian|Age: 1400Ma||||||
14818|Pandurra Formation|22645|6|Mentioned|Fig5 P206|||||||||
14818|Pandurra Formation|22677|5|Briefly described|p734, Fig.2 p735|Mesoproterozoic|Mesoproterozoic|Age of unit 1424+/-51 Ma. See also p733, Fig.1 p734||||||
14818|Pandurra Formation|22829|6|Mentioned|P16|||Maximum thickness 4.5m||||||
14818|Pandurra Formation|22925|6|Mentioned|48|||Overlying unit Tapley Hill Formation||||||
14818|Pandurra Formation|22950|6|Mentioned|p47|||||||||
14818|Pandurra Formation|23054|6|Mentioned|p14|||||||||
14818|Pandurra Formation|23282|6|Mentioned|p68|||||||||
14818|Pandurra Formation|23481|5|Briefly described|p19 Fig 1|||Geological Province: Gawler Craton.||||||
14818|Pandurra Formation|23519|5|Briefly described|p138|||Geological Province: Gawler Craton.||||||
14818|Pandurra Formation|23719|4|Described|p24|Mesoproterozoic|Mesoproterozoic|See also page 22 Table 6. Underlain by Moonabie Formation. Geological Province: Gawler Craton. Max. thickness: >200 m.||||||26-FEB-08
14818|Pandurra Formation|23791|5|Briefly described|p3 Fig. 2|Mesoproterozoic|Mesoproterozoic|Geological Province: Gawler Craton.||||||
14818|Pandurra Formation|23805|5|Briefly described|p4 Fig. 1|Mesoproterozoic|Mesoproterozoic|Geological Province: Gawler Craton.||||||
14818|Pandurra Formation|23818|5|Briefly described|p54|||Underlying unit: Roopena Volcanics (unconformable).||||||
14818|Pandurra Formation|24175|5|Briefly described|p6|Mesoproterozoic|Mesoproterozoic|||||||
14818|Pandurra Formation|24261|5|Briefly described|p1047 Fig.1|Neoproterozoic|Mesoproterozoic|Geological Province: Gawler Craton||||||
14818|Pandurra Formation|24321|5|Briefly described|Map legend|Proterozoic|Proterozoic|||||||
14818|Pandurra Formation|24362|5|Briefly described|p42|||pre-Adelaidean fluviatile sandstone.  Overlain by Whyalla Sandstone. Max. thickness: ~1000m.||||||22-MAR-05
14818|Pandurra Formation|24422|5|Briefly described|p84 Fig. 1|Mesoproterozoic|Mesoproterozoic|Age: ca. 1450 Ma. Geological Province: Gawler Craton.||||||
14818|Pandurra Formation|24472|5|Briefly described|p5 Tb.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Harris Greenstone Domain, Gawler Craton.||||||
14818|Pandurra Formation|24583|6|Mentioned|p12|Mesoproterozoic|Mesoproterozoic|Age: 1424+/-51Ma.||||||
14818|Pandurra Formation|24597|5|Briefly described|p526 Fig. 1|Mesoproterozoic|Mesoproterozoic|Geological Province: Cariewerloo Basin (Gawler Craton).||||||
14818|Pandurra Formation|29838|6|Mentioned|p4|||||||||
14818|Pandurra Formation|30237|6|Mentioned|Fig.1|||||||||
14818|Pandurra Formation|30310|6|Mentioned|p9|||Mineralisation||||||
14818|Pandurra Formation|30801|6|Mentioned|p5|||Willouran. Table P5-6||||||
14818|Pandurra Formation|30806|6|Mentioned|Fig.1|||||||||
14818|Pandurra Formation|30807|6|Mentioned|p103|||Suggested map symbol||||||
14818|Pandurra Formation|30845|6|Mentioned|Fig.1|||||||||
14818|Pandurra Formation|31313|5|Briefly described|p196|||||||||
14818|Pandurra Formation|31324|5|Briefly described|p158|||||||||
14818|Pandurra Formation|31395|6|Mentioned|p64|||||||||
14818|Pandurra Formation|31540|4|Described|p8|||See also p7.||||||02-JUN-09
14818|Pandurra Formation|31541|6|Mentioned|p545|||||||||
14818|Pandurra Formation|31719|4|Described|p16|||Proterozoic. Pernatty grit of Johns (1968).||||||
14818|Pandurra Formation|32458|6|Mentioned|p10|||||||||
14818|Pandurra Formation|32507|6|Mentioned|Table 3|||||||||
14818|Pandurra Formation|33468|6|Mentioned|Fig.6|||Adelaidean||||||
14818|Pandurra Formation|33470|6|Mentioned|Table 1|||||||||
14818|Pandurra Formation|33474|6|Mentioned|Fig.4|||||||||
14818|Pandurra Formation|33479|6|Mentioned|Fig.1|||||||||
14818|Pandurra Formation|34116|4|Described|p13|||Proterozoic. See also PP14-17||||||
14818|Pandurra Formation|34319|6|Mentioned|p69|||Torrensian - Willouran||||||
14818|Pandurra Formation|34535|6|Mentioned|p55|||Equiv. Upper Callanna Beds||||||
14818|Pandurra Formation|34537|6|Mentioned|Fig.7|||||||||
14818|Pandurra Formation|34685|6|Mentioned|p353|||||||||
14818|Pandurra Formation|34831|6|Mentioned|p95|||||||||
14818|Pandurra Formation|34984|6|Mentioned|p322|||||||||
14818|Pandurra Formation|35002|6|Mentioned|p28|||||||||
14818|Pandurra Formation|35135|6|Mentioned|p4|||||||||
14818|Pandurra Formation|35255|5|Briefly described|p9|||See also P13 and Fig.3.||||||
14818|Pandurra Formation|35270|4|Described|p6|||||||||
14818|Pandurra Formation|35298|6|Mentioned|Fig.1|||||||||
14818|Pandurra Formation|35678|6|Mentioned|p64|||Summary geological logs.||||||
14818|Pandurra Formation|35706|6|Mentioned|Fig.1|||||||||
14818|Pandurra Formation|35772|6|Mentioned|p9|||||||||
14818|Pandurra Formation|36185|6|Mentioned|Fig.9|||||||||
14818|Pandurra Formation|36507|6|Mentioned|Fig.2|||||||||
14818|Pandurra Formation|36733|6|Mentioned|p49|||||||||
14818|Pandurra Formation|37238|6|Mentioned|p368|||||||||
14818|Pandurra Formation|37461|4|Described|p335|||See also Table 5.I and Fig.5.11||||||
14818|Pandurra Formation|37621|6|Mentioned|p12|||||||||
14818|Pandurra Formation|38157|6|Mentioned|Table II|||||||||
14818|Pandurra Formation|38581|4|Described|p253|||||||||
14818|Pandurra Formation|39344|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
14818|Pandurra Formation|39349|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
14818|Pandurra Formation|39352|6|Mentioned|Map legend|Adelaidean|Adelaidean|Willouran||||||
14818|Pandurra Formation|39490|6|Mentioned|p11|||||||||
14818|Pandurra Formation|39724|6|Mentioned|p107|||||||||
14818|Pandurra Formation|39762|6|Mentioned|Table 1|||||||||
14818|Pandurra Formation|39802|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
14818|Pandurra Formation|39866|5|Briefly described|p267|||||||||
14818|Pandurra Formation|39901|4|Described|p11|||||||||
14818|Pandurra Formation|40257|6|Mentioned|p287|||||||||
14818|Pandurra Formation|40294|6|Mentioned|p41|||See also P43||||||
14818|Pandurra Formation|40430|6|Mentioned|Table 2|||See also Fig.1||||||
14818|Pandurra Formation|40445|6|Mentioned|p53|||||||||
14818|Pandurra Formation|40448|5|Briefly described|p36|||See also P37.||||||
14818|Pandurra Formation|40644|5|Briefly described|p121, p124 Fig. 3||Mesoproterozoic|Clastic sediments. Maximum age of sedimentation is ca.1420Ma.  See also p135.||||||13-AUG-08
14818|Pandurra Formation|41364|6|Mentioned|p156|||||||||
14818|Pandurra Formation|41402|4|Described|p36|||||||||
14818|Pandurra Formation|41403|6|Mentioned|p44|||||||||
14818|Pandurra Formation|41405|6|Mentioned|p126|||See also P128||||||
14818|Pandurra Formation|41493|6|Mentioned|Table 1|||||||||
14818|Pandurra Formation|41526|6|Mentioned|p22|||See alsp P47||||||
14818|Pandurra Formation|41609|6|Mentioned|Fig.1|||||||||
14818|Pandurra Formation|41667|5|Briefly described|p6|||||||||
14818|Pandurra Formation|41972|6|Mentioned|p367|||||||||
14818|Pandurra Formation|42088|5|Briefly described|p544|||See also Fig.2 P546||||||
14818|Pandurra Formation|42167|6|Mentioned|Fig.2 P115|||||||||
14818|Pandurra Formation|42168|4|Described|p122|||||||||
14818|Pandurra Formation|42222|6|Mentioned|p16|||||||||
14818|Pandurra Formation|42223|6|Mentioned|Fig.2 P36|||||||||
14818|Pandurra Formation|42235|6|Mentioned|p131|||||||||
14818|Pandurra Formation|42283|6|Mentioned|p86|||||||||
14818|Pandurra Formation|42357|6|Mentioned|p8|||||||||
14818|Pandurra Formation|42465|5|Briefly described|Map legend|||||||||
14818|Pandurra Formation|42468|5|Briefly described|p3|||||||||
14818|Pandurra Formation|42469|4|Described|p21, p10|||In the Cariewerloo Basin. Age: Mesoproterozoic.||||||26-FEB-08
14818|Pandurra Formation|42546|5|Briefly described|Map legend||Mesoproterozoic|||||||
14818|Pandurra Formation|42721|5|Briefly described|map legend|Torrensian||||||||
14818|Pandurra Formation|42723|5|Briefly described|map legend|Willouran||||||||
14818|Pandurra Formation|42736|5|Briefly described|map legend|Neoproterozoic||||||||
14818|Pandurra Formation|42775|6|Mentioned|Fig.13 P323|||||||||
14818|Pandurra Formation|43025|5|Briefly described|p574|||||||||
14818|Pandurra Formation|43048|4|Described|Table 1.|||||||||
14818|Pandurra Formation|43052|3|Fully described|p139|||At least 1424+/-51 Ma.||||||26-FEB-08
14818|Pandurra Formation|43053|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Fluvial sandstone, minor siltstone.||||||26-MAY-05
14818|Pandurra Formation|43094|4|Described|p33,Table 5|||||||||
14818|Pandurra Formation|43141|6|Mentioned|p63,Fig.1|||||||||
14818|Pandurra Formation|43258|5|Briefly described|Map Legend||Mesoproterozoic|||||||
14818|Pandurra Formation|43298|5|Briefly described|Map Legend||Mesoproterozoic|||||||
14818|Pandurra Formation|44133|5|Briefly described|p75 Fig. 8.13|||Geological Province: Arckaringa Basin.||||||
14818|Pandurra Formation|44660|14|Not recorded|map legend||Proterozoic|Proterozoic, lithology.||||||
14818|Pandurra Formation|44934|5|Briefly described|Map Legend||Adelaidean|||||||
14818|Pandurra Formation|44935|5|Briefly described|Map Legend||Proterozoic|||||||
14818|Pandurra Formation|47004|6|Mentioned|p328|||||||||
14818|Pandurra Formation|47012|6|Mentioned|p332|||||||||
14818|Pandurra Formation|50225|5|Briefly described|p406 Fig. 10, p407|Mesoproterozoic|Mesoproterozoic|||||||07-FEB-11
14818|Pandurra Formation|60953|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Age: >1424Ma. Fluvial sandstone, minor siltstone.||||||
14818|Pandurra Formation|60954|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Geological Province: Gawler Craton.||||||31-MAY-05
14818|Pandurra Formation|60955|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Red-purple sandstones, medium to coarse grained, kaolinitic reddish,-brown siltstones with bleached spots.||||||22-APR-05
14818|Pandurra Formation|61070|6|Mentioned|Map Legend|Mesoproterozoic|Mesoproterozoic|Possibly equivalent to Blue Range beds.||||||12-JAN-10
14818|Pandurra Formation|61108|5|Briefly described|map legend|Mesoproterozoic|Mesoproterozoic|Fluvial sandstone, minor siltstone. Age: >1424 Ma.||||||
14818|Pandurra Formation|61307|5|Briefly described|p36 Fig. 17|Mesoproterozoic|Mesoproterozoic|Geological Province: Gawler Craton. See also p39 Fig. 19, p43.||||||
14818|Pandurra Formation|62453|5|Briefly described|p15|Mesoproterozoic|Mesoproterozoic|||||||
14818|Pandurra Formation|62664|5|Briefly described|p138 Fig.2, p139. |Mesoproterozoic|Mesoproterozoic|Youngest intrusion into the pre-Adelaidean Adelaide Geosyncline basement.|1424 +/- 51 Ma (Fanning et al. 1983)|||Unconformably overlies Archean to Mesoproterozoic basement. Is unconformably overlain by Callanna Group.|Basalt.|
14818|Pandurra Formation|62727|5|Briefly described|p9|Mesoproterozoic|Mesoproterozoic|Sandstones. Unconformably overlies Hutchinson Group, Hiltaba Suite granitoids and Gawler Range Volcanics. Uranium-prospective at the margins of the Cariewerloo Basin margin.||||||
14818|Pandurra Formation|62869|5|Briefly described|p630|||Includes redbeds. Underlies Beda Volcanics. In the eastern Eyre Peninsula area.||||||28-NOV-06
14818|Pandurra Formation|62893|6|Mentioned|p15|||Possibly equivalent to the Blue Range Beds.||||||
14818|Pandurra Formation|63067|5|Briefly described|p2 Fig. 1|Mesoproterozoic|Mesoproterozoic|Age: >1425Ma. Sandstone, siltstone, shale, conglomerate.||||||
14818|Pandurra Formation|63224|5|Briefly described|p6 Fig. 2|Mesoproterozoic|Mesoproterozoic|Geological Province: Cariewerloo Basin. Sandstone. Age is Middle Mesoproterozoic.||||||07-FEB-08
14818|Pandurra Formation|63866|5|Briefly described|p7, p9, p21, p30|Calymmian|Calymmian|Olympic Domain, Gawler Craton. An additional Rb-Sr age of 1421+/- 54 Ma is provided, also from Fanning et al., 1983.|1424 +/- 51 (Rb-Sr, Fanning et al., 1983)|||Overlies the Gawler Range Volcanics.||
14818|Pandurra Formation|64131|5|Briefly described|p1400, p1410 Tb.1, p1404, p1408-1410  |Mesoproterozoic|Mesoproterozoic|Petrophysical properties. Inferred minimum depositional age.|1424 +/- 51 Ma (Fanning et al., 1983).||||Fluviatile red beds.|
14818|Pandurra Formation|64132|6|Mentioned|p1420 Fig.4, p1424 Fig.6. |||||||Unconformably overlies Wallaroo Group and Gawler Range Volcanics. Nonconformably overlies Donington Suite.||
14818|Pandurra Formation|64133|5|Briefly described|p1443 |Mesoproterozoic|Mesoproterozoic|Eastern Gawler Craton.||||||
14818|Pandurra Formation|64724|5|Briefly described|p48|Calymmian|Calymmian|Cariewerloo Basin (Gawler Craton) unit|~1450 Ma.|||||02-APR-12
14818|Pandurra Formation|65376|5|Briefly described|p9 Fig.1.2, p139.|Mesoproterozoic|Mesoproterozoic|312m thick at Emmie Bluff prospect.||||Is overlain by Tapley Hill Formation.|Fluvial sandstone.|
14818|Pandurra Formation|65390|4|Described|p10, p18, p23 Fig.3|Calymmian||Olympic Domain, Gawler Craton. A widespread, thick sequence of undeformed arenaceous red bed sediments. Unconformably overlies Gawler Range Volcanics and Hiltaba Suite. Unconformably underlies Beda Volcanics and Backy Point Formation. Minimum depositional age of 1424 +/- 51 Ma from Rb-Sr geochronology (Fanning et al. 1983). Hosts copper mineralisation, eg Mount Gunson.||||||
14818|Pandurra Formation|65483|6|Mentioned|p19|Mesoproterozoic|Mesoproterozoic|Part of Stuart Shelf sequence.||||||
14818|Pandurra Formation|65922|5|Briefly described|p26, p29 Fig. 6|Calymmian|Calymmian|Fig.6 indicates age of ~1505 - 1450 Ma. Rounded to subrounded pebbles and cobbles of quartzite (?Pandurra Formation) making up Tertiary talus.||||||20-MAR-15
14818|Pandurra Formation|66302|5|Briefly described|p33, p34, p43, p47|Calymmian|Statherian|Spencer and Olympic Domains, Gawler Craton. Ages are SHRIMP maximum depositional ages derived from Fraser and Neumann (2010).|1756 +/- 5 Ma to 1575 +/- 5 Ma||||Medium to coarse-grained quartz-rich and lithic-rich sandstone with pebble conglomerate and shale.|
14818|Pandurra Formation|66520|6|Mentioned|p10, p18.|||Gawler Craton. Forms a ~650 m cover over Archean basement rocks.||||||
14818|Pandurra Formation|66537|4|Described|p9-15.|Mesoproterozoic|Mesoproterozoic|Deposited in intracratonic Cariewerloo Basin. Sediments derived from elevated Gawler Range Volcanics to the west of the Cariewerloo Basin. Four informal members have been recognised. Potential for unconformity-related uranium deposit.|Minimum depositional age of 1424 +/- 51 Ma.|||Unconformably overlies northeastern Gawler Craton.|Unmetamorphosed, dominantly fluvial redbed sediments: medium- to coarse-grained, poorly sorted, subangular quartz and lithic sandstone; minor conglomerate, mudstone, siltstone. Large-scale cross-bedding; liesegang banding.|
14818|Pandurra Formation|67027|4|Described|pp347-357.|Mesoproterozoic|Mesoproterozoic|Cariewerloo Basin, northeastern Gawler Craton. Unmetamorphosed, low-dipping fluvial deposits; 200 - 1600 m thick. Age is poorly constrained; Gawler Range Volcanics and Hiltaba Suite appear the dominant sources of sediments. A whole-rock siltstone Rb-Sr isochron age of 1424 +/- 51 Ma (Fanning et al. 1983) was interpreted as a maximum deposition age. Suggested correlative of Blue Range Beds. Palaeomagnetic data is discussed in detail and a pole position is plotted on the Mesoproterozoic APWP for Australia.|<1.59 Ga to c. 1.1 Ga.|||Overlies Gawler Range Volcanics and Hiltaba Suite. Is intruded by Gairdner dyke swarm. Is overlain by Beda Volcanics.|Fluvial red beds. Basal conglomerate; coarse-grained, poorly-sorted, lithic and feldspathic sandstones with conglomerate bands; local shale and siltstone. Silicification near top, and cross-bedding, common. Local Liesegang banding.|
14818|Pandurra Formation|67030|5|Briefly described|p408|||Text specifies age as pre-Adelaidean, so minimum age would be Cryogenian or older.||||Intruded by Gairdner Dykes.||26-APR-12
14818|Pandurra Formation|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Southern Gawler Craton.|1575 +/- 5 Ma (maximum depositional age).|||||
14818|Pandurra Formation|67536|5|Briefly described|Map Legend|Ectasian|Calymmian|Cariewerloo Basin; mapped as M-p. Rocks mapped as equivalent to the Pandurra Formation in the Curnamona Province are mapped as ?M-p and include sandstone, siltstone and shale. The note gives the age as a maximum, but it should be minimum (cf RefID 43052).|ca. 1424 +/- 51 Ma (min, Rb-Sr)||||Redbed sandstone, minor siltstone.|01-APR-14
14818|Pandurra Formation|67870|5|Briefly described|p13, p18, p20, p24|Mesoproterozoic|Mesoproterozoic|Low seismic relectivity.||||Overlies Gawler Range Volcanics. Is overlain by Callanna Group.||
14818|Pandurra Formation|68131|5|Briefly described|p2 Fig.1, p89|Mesoproterozoic|Mesoproterozoic|Fluvial deposits.|||||Sandstone.|
14818|Pandurra Formation|68158|6|Mentioned|p4||||||||Medium-grained and gritty red sandstones, cross-bedded, conglomeratic near base; mottled red-purple basal conglomerate.|
14818|Pandurra Formation|68714|6|Mentioned|p16, p17 Fig.7|||Cariewerloo Basin. A large area of high dissolved Vanadium correlates to the edge of the Pandurra Formation where it laps on the Gawler Range Volcanics.||||Underlain by the Gawler Range Volcanics.||
14818|Pandurra Formation|69654|6|Mentioned|p1, 4, 11, 25|||Teale and Flint (1995). Curnamona Province.|1424 +/- 51 Ma (Fanning et al., 1983).||||A potential [equivalent] section, intersected in Bumbarlow 1 core, is described in some detail.|
14818|Pandurra Formation|69666|5|Briefly described|p24-29, p31, p33, p39|Mesoproterozoic|Mesoproterozoic|Stuart Shelf. Source of some red sandstone and arkose sediments in the Backy Point Formation. U-Pb zircon maximum depositional age. Also 1424 +/- 51 Ma (Rb-Sr, siltstone and shale: Fanning et al., 1983).|< 1575 +/- 5 Ma (Fraser and Neumann, 2010).|||Overlies Roopena Volcanics. Is overlain by Beda Basalt.||
14818|Pandurra Formation|69928|6|Mentioned|p224|Mesoproterozoic|Mesoproterozoic|Northern Stuart Shelf and Gawler Craton. Postulated deposition resulting from Anmatjira Event (1500-1400 Ma) in the Arunta Inlier.||||||
14818|Pandurra Formation|69946|6|Mentioned|p38|||Pre-Adelaidean.||||||
14818|Pandurra Formation|70333|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic||||||Sandstone, shale and siltstone, arenaceous, red beds.|
14818|Pandurra Formation|70334|4|Described|p2-3,10,12,17-18,39,44,47,51,53,76|Statherian|Statherian|Geological province: Gawler Craton. Of Cariewerloo Basin. Thick unit of relatively flat-lying arenaceous fluvial (possibly including alluvial dan, deltaic and lacustrine) sediments. Extends eastward from CULTANA beneath the Stuart Shelf, but has not been observed in the Cultana Inlier (either not deposited in this area or eroded prior to Beda Basalt and Backy Point Formation deposition). Cowley (1991b) inferred Pandurra Formation deposition to precede NW-trending bounding faults of the Cariewerloo Basin, occurring in a down-warped portion of the Gawler Craton, based on the homogeneity of internal stratigraphic geometry and facies irrespective of depth to underlying basement. Probably eroded from the Cultana Inlier during uplift of Cultana Inlier. Fraser and Neumann (2010) provided a maximum depositional age of 1575+\-5 Ma, consistent with derivation from Gawler Range Volcanics, and possible local derivations from Moonabie Formation. May host unconformity-related uranium. See also p82-p83,88-p90.|1575 Ma (max dep age)|||Underlain unconformably by Moonabie Formation. Intruded by Gairdner Dolerite.|Mottled medium- to coarse-grained, poorly sorted purple and red, quartzitic and lithic sandstone with lesser conglomerate and siltstone, chert, ferruginous chert, ironstone, muscovite and felsic volcanics.|14-OCT-19
14818|Pandurra Formation|70406|5|Briefly described|p124|Mesoproterozoic|Mesoproterozoic|Gawler Craton.||||||
14818|Pandurra Formation|70511|6|Mentioned|p86|Mesoproterozoic|Mesoproterozoic|Eastern Gawler Craton.|1424 +/- 51 Ma (Fanning et al., 1983).||||Continental sedimentary rocks. Not deformed nor metamorphosed.|
14818|Pandurra Formation|70659|5|Briefly described|p9, p10-11, p14|Mesoproterozoic|Mesoproterozoic|NW margin of the Gawler Craton. Age shown as Neoproterozoic on p10.||||Overlies Roopena Basalt.|Mottled medium- to coarse-grained, poorly sorted purple and red sandstones. Basal conglomerate.|
14818|Pandurra Formation|70721|6|Mentioned|p64|Mesoproterozoic|Mesoproterozoic|||||||
14818|Pandurra Formation|70738|6|Mentioned|p186-187|Mesoproterozoic|Mesoproterozoic|Cariewerloo Basin, Gawler Craton.|c.1450-1424 Ma.|||||
14818|Pandurra Formation|70816|6|Mentioned|p3|Neoproterozoic|Neoproterozoic|Gawler Ranges region.||||||
14818|Pandurra Formation|70948|6|Mentioned|p974|Neoproterozoic|Neoproterozoic|Geological province: Gawler Craton.||||||
14818|Pandurra Formation|71037|5|Briefly described|p21,  p22-23 Fig.2, p27 Fig.6, p29|Mesoproterozoic|Mesoproterozoic|Includes unnamed subunit of basal pebble to boulder conglomerate.||||Shown as younger than Gawler Range Volcanics and older than Backy Point Point Formation and Gairdner Dolerite.|Reddish-brown cross-bedded sandstone, minor shale, siltstone, conglomerate with basal pebble to boulder conglomerate.|
14818|Pandurra Formation|71043|5|Briefly described|p106, p108, p116-117|Mesoproterozoic|Mesoproterozoic|Cariewerloo Basin, Gawler Craton. Red bed-dominated clastic fluvial deposits. 1181m thick overlying tonalite basement in drillhole SH 7. Rb-Sr isochron age determination by Fanning et al. (1983).|1424 +/- 51 Ma (maximum depositional age).||||Pebbly sandstone, conglomerate, siltstone, minor shale.|
14818|Pandurra Formation|71129|4|Described|p1,14,21,35,64,85,89-90,92-98,101|Calymmian|Calymmian|Of Cariewerloo Basin. Typically poorly exposed, outcrops occur around Carriewerloo HS and as S-SE trending belt of low hills from O'Reily Dam to Red Rock Hill. Thickness at type section: over 500m on eastern side (hanging wall) of Wizzo Fault (Thomson et al., 1976, Preiss, 1987); over 400m in ROOPENA DDH 5, which did not penetrate base of Pandurra Formation. Fluvial redbed sedimentation into a faulted Mesoproterozoic intracratonic basin (Cariewerloo Basin). Based on homegeneity in internal stratigraphy and sedimentary facies irrespective of depth to basement, interpreted to have been deposited in a downwarped part of the Gawler Craton. Basal conglomerates reflect deposition as proximal colluvial-alluvial-fluvial sediments on a basin floor with marked basement topography, transitioning into braided fluvial environments. Paleocurrent indicators show a dominantly easterly transport.  Juxtaposed against Moonabie Formation via Red Rock Fault. Geochronogical results include maximum depositional zircon age of 1575+\-5 Ma (Fraser and neumann 2010), whole rock Rb-Sr isochron age of 1424+\-5 Ma (Fanning et al., 1983), likely representing minimum depositional age. There remains uncertainties whether the basal conglomerates could be older i.e. correlatives to the Corruna Conglomerate, based on mapping and geological descriptions by Coats et al (1983). See also p105,107,109,112,114-115,122,126,141-142,149,177,p180, 182-184,187,199,207,225,227,231.|c. 1420 Ma|||Overlain by Tapley Hill Formation, Backy Point Formation, Beda Basalt, Moonlight Conglomerate. Underlain unconformably by Moonabie Formation or Broadview Schist or Roopena Basalt or Eucarro Rhyolite.|Reddish-brown crossbedded sandstones with lesser conglomerates, siltstones and shales.|13-NOV-19
14818|Pandurra Formation|71130|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Maximum depositional age.|< 1575 +/- 5 Ma (Fraser and Neumann, 2010).||||Reddish-brown cross-bedded sandstone, minor shale, siltstone, conglomerate.|
14818|Pandurra Formation|71131|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Basal conglomerate is mapped separately.|||||Reddish-brown cross-bedded sandstone, minor shale, siltstone, conglomerate. Basal pebble to boulder conglomerate.|
14818|Pandurra Formation|71235|6|Mentioned|p3-p5|Mesoproterozoic|Mesoproterozoic|||||||
14818|Pandurra Formation|71236|6|Mentioned|p28, p29 fig 24|||||||||
14818|Pandurra Formation|71317|6|Mentioned|p177|||||||||
14818|Pandurra Formation|71341|6|Mentioned|p182 fig 4|||||||||
14818|Pandurra Formation|71414|6|Mentioned|p42 Fig 1|Mesoproterozoic|Mesoproterozoic|Geological province: Gawler Craton.||||||
14818|Pandurra Formation|71536|5|Briefly described|p119, p121|||At least 1000 metres thick.|||||Conglomerate and sandstone.|
14818|Pandurra Formation|71559|6|Mentioned|p15 Fig 1|Mesoproterozoic|Mesoproterozoic|Geological province: Gawler Craton.||||||
14818|Pandurra Formation|71712|3|Fully described|p409-413, p415-424|Calymmian|Calymmian|Of Cariewerloo Basin. Maximum thickness: 2000m, within half-graben-like depocentres in fluvial and lacustrine environments. Unmetamorphosed, relatively flat-flying Mesoproterozoic siliciclastic unit deposited on northeastern Gawler Craton. Records first major interval of basin formation following craton assembly. Maximum age of 1575 Ma. Minimum depositional age of 1424 +\- 51 Ma posulated by Fanning, Flint and Preiss (1983) using Rb\Sr geochron.  Minimum age of sedimentation determined through 40Ar/39Ar heating. Detailed lithofacies are provided in Table 1 p412. Detailed mineral paragenesis, lithogeochemistry, stable isotopic analysis and Ar/Ar geochronology is described from p413-419. Detailed analyses of uranium prospectivity described from p421-423. 4 lithofacies discussed.Intruded by Gairdner Dolerite|1575-1490 Ma||4 lithofacies discussed. Differences between upper and lower parts discussed p409, 413, 415, 424.|Unconformably overlies the Tunkillia Suite, Nuyts Volcanics and St Peter Suite. Overlain by Umberatana and Wilpena groups and Beda Basalt, Tapley Hill Formation, Whyalla Sandstone.|Lithic, quartz pebble conglomerate; lithic, qtz pebble/granule arenite; wacke w rock and  qtz clasts. med/coarse, mod. sorted sublitharenite/lithic arenite, micaceous maroon siltstone/mudstone. Maroon siltstone/mudstone and  fine lithic arenite.|31-MAR-20
14818|Pandurra Formation|71859|6|Mentioned|p6|Mesoproterozoic|Mesoproterozoic|Gawler Craton. Outcrops on the Eyre Peninsula.||||||
14818|Pandurra Formation|71862|6|Mentioned|p8, p12|Mesoproterozoic|Mesoproterozoic|||||||
14818|Pandurra Formation|71895|4|Described|p10, p11 fig 2, p24, p29, p38|Mesoproterozoic|Mesoproterozoic|Directly overlies proterozoic crystalline basement. This unit shows dramatic thickness variations throughout the area. Spectral analysis is provided. See also  p52-p53, p61-p63, p90, p116, p142-p144, p150-p151, APP1. p6-p7, APP1. p10, APP1. p14-p17, APP4. p4, APP4. p8,  APP5. p15, p60, p105, p141. See also APP6. p173, p176-p177, p179-p180, APP8. p201-p203. Petrographic descriptions for numerous samples are provided in APP5. Intersected in drillholes CDDD01, WDDD01 and PDDD01.|c. 1450 Ma|||Intruded by the Gairdner Dolerite. Overlain by the Beda Basalt.|Medium- to coarse-grained, poorly sorted, sub-angular, quartz and lithic sandstone, which includes moderately to well-sorted, very fine to medium-grained sandstone, pebble conglomerate and siltstone horizons.|
14818|Pandurra Formation|72089|6|Mentioned|p3|Mesoproterozoic|Mesoproterozoic|Gawler Craton.||||||
14818|Pandurra Formation|72090|5|Briefly described|p9, p95|Mesoproterozoic|Mesoproterozoic|Gawler Craton.|||||Thick, red-bed sequence of mostly sandstone and conglomerate.|
14818|Pandurra Formation|72237|5|Briefly described|p29|Mesoproterozoic|Mesoproterozoic|Geological province: Gawler Craton.||Unit of Gawler Range Volcanics.||||
14818|Pandurra Formation|72247|5|Briefly described|p39-43|Mesoproterozoic|Neoproterozoic|Of Adelaide Geosyncline. Contains minor veinlets of copper sulfide following joint and bedding planes.||||Overlain disconformably by Tapley Hill Formation or Whyalla Sandstone.|Red (Fe-rich) quartzites and sandstones, grit.|
14818|Pandurra Formation|72463|6|Mentioned|p2|Mesoproterozoic|Mesoproterozoic|||||||
14818|Pandurra Formation|73103|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic||||||Sandstone, shale and siltstone, arenaceous, red beds.|
14818|Pandurra Formation|73110|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|The basal conglomerate is mapped separately.|||||Sandstone, shale and siltstone, arenaceous, red beds. Basal red/purple mottled conglomerate.|
14818|Pandurra Formation|73129|6|Mentioned|p46|Mesoproterozoic|Mesoproterozoic|Cariewerloo Basin. Fluvial.|1424 +/- 51 Ma minimum age|||||
14818|Pandurra Formation|73130|6|Mentioned|[poster] Fig. 1|Mesoproterozoic|Mesoproterozoic|||||||28-OCT-22
14818|Pandurra Formation|73162|6|Mentioned|p450 Fig.2, p452 Fig.3, p457|Mesoproterozoic|Mesoproterozoic|||||||
14818|Pandurra Formation|73166|6|Mentioned|p644, 652, 656|Mesoproterozoic|Mesoproterozoic|Gawler Craton. Uncomfortably overlies the Olympic Cu-Au Province. Base of the formation is highly variable, brecciated in places, suggests significant faulting in the Acropolis area.|1440 Ma diagenesis age.|||||
14818|Pandurra Formation|73227|5|Briefly described|p23-25, p27, p29, p36-37|Ectasian|Calymmian|Sediment-hosted, stratabound Cu sulfide deposits are known to occur at the upper boundary with the overlying Whyalla Sandstone. Geochron from Fanning et al. (1983). Diagenetic illite in the base of the unit dated to c. 1490 Ma via Ar-Ar. Silicified, brecciated, and mineralized at Cattle Grid mine to form Cattle Grid Breccia. Contains [informal] members including a coarse-grained lowermost member (Member 1), which has bleached, reduced zones.|1424 +/- 51 Ma Rb-Sr|||Overlain by Beda Basalt, and Tapley Hill Formation, and unconformably by Whyalla Sandstone. Intruded by Gairdner Dolerite.|Redbeds / red sandstones.|
14818|Pandurra Formation|73230|6|Mentioned|p14|||||||Unconformably underlain by Sloan Hill Tonalite.||
14818|Pandurra Formation|73234|6|Mentioned|p4-5, p19-20|Calymmian|Calymmian|Cariewerloo Basin. Widely exposed on Six Mile Hill. Fluviolacustrine redbed sediments.|c. 1500 Ma|||||
14818|Pandurra Formation|74361|5|Briefly described|p164, 166, 173, 176|Mesoproterozoic|Mesoproterozoic|Gawler Craton.|c.1440 Ma.|||Unconformably overlay Roxby Downs Granite and Olympic Dam Breccia Complex.|Red beds.|
14818|Pandurra Formation|74367|6|Mentioned|p23|Mesoproterozoic|Mesoproterozoic|||||||
14844|Pantoulbie Formation|29664|2|Defined|p3|late Tertiary|late Tertiary|||||||
14844|Pantoulbie Formation|40448|5|Briefly described|p43|||||||||
14844|Pantoulbie Formation|42292|5|Briefly described|Fig.3 P12|||||||||
14844|Pantoulbie Formation|43049|6|Mentioned|p23|||||||||
14844|Pantoulbie Formation|61155|5|Briefly described|p17|Late Pliocene|Early Pliocene|Age: 4-2.5Ma. Thickness: 40m. Geological Province: Polda Basin, Eyre Peninsula.||||||
14844|Pantoulbie Formation|62898|6|Mentioned|p204|Tertiary|Tertiary|Of Barnett (1978), Parker et al (1985).||||||
14854|Parabarana Sandstone|23394|5|Briefly described|Map legend|Cretaceous|Jurassic|||||||
14854|Parabarana Sandstone|23478|5|Briefly described|p27|Cretaceous|Cretaceous|||||||
14854|Parabarana Sandstone|23818|6|Mentioned|p141 Fig.65|||Geological Province: Great Artesian Basin. Of the Pelican Well Formation.||||||
14854|Parabarana Sandstone|24176|5|Briefly described|p22 Tb. 1, p19|Early Cretaceous|Early Cretaceous|Kaolinitic sandstone and conglomerate; Aptian flora and fauna.  Geological Province: Mount Painter Province.||||||
14854|Parabarana Sandstone|24392|5|Briefly described|p139, p144 Appendix 1|||Regionally correlative with Cadna-owie Formation (Frakes et al, 1995; Sheard et al, 2000). See also page 140 Fig.1. Geological Province: Eromanga Basin.||||||
14854|Parabarana Sandstone|30176|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
14854|Parabarana Sandstone|30177|6|Mentioned|p103|||Cretaceous age||||||
14854|Parabarana Sandstone|30807|6|Mentioned|p102|||Suggested map symbol||||||
14854|Parabarana Sandstone|33165|6|Mentioned|Chart|||Correlation chart only||||||
14854|Parabarana Sandstone|33828|6|Mentioned|Table 3|||||||||
14854|Parabarana Sandstone|33939|5|Briefly described|p413|||of the Pelican Well Fm?||||||18-MAR-08
14854|Parabarana Sandstone|34611|4|Described|p153|||Correlation chart. Lower Cretaceous. p152.||||||23-JAN-19
14854|Parabarana Sandstone|36552|6|Mentioned|p59|||||||||
14854|Parabarana Sandstone|36571|6|Mentioned|Table 4|||||||||
14854|Parabarana Sandstone|38007|6|Mentioned|p36|||||||||
14854|Parabarana Sandstone|38068|6|Mentioned|p71|||||||||
14854|Parabarana Sandstone|39211|6|Mentioned|p23|||||||||
14854|Parabarana Sandstone|40926|6|Mentioned|Table 2|||||||||
14854|Parabarana Sandstone|41085|6|Mentioned|Fig.1|||||||||
14854|Parabarana Sandstone|44133|5|Briefly described|p112-113|||||||||
14854|Parabarana Sandstone|46791|6|Mentioned|p42|||||||||
14854|Parabarana Sandstone|60953|5|Briefly described|Map Legend|Cretaceous|Cretaceous|||||||
14854|Parabarana Sandstone|61108|5|Briefly described|map legend|Cretaceous|Cretaceous|Transitional, non-marine to marine sandstone, siltstone, calcareous sandstone and pebbly sandstone.||||||
14854|Parabarana Sandstone|65925|5|Briefly described|Appendix 2.||||||||Calcareous sandstone with clasts of quartz, quartzite and porphyry; sand, gravel and shale. U shaped burrows and other fossils.|
14854|Parabarana Sandstone|66303|6|Mentioned|pp27-28.|Early Cretaceous|Early Cretaceous|Stratigraphically equivalent to Cadna-owie Formation.||||||
14854|Parabarana Sandstone|66518|5|Briefly described|p19.|Cretaceous|Cretaceous|Eromanga Basin.||||Is overlain unconformably by Bulldog Shale. Is age-equivalent to Cadna-owie Formation in southern Eromanga Basin.||06-FEB-14
14854|Parabarana Sandstone|66623|6|Mentioned|p251.|||Ludbrook (1966). Laterally equivalent to the Cadna-owie Formation.||||||
14854|Parabarana Sandstone|68068|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Eromanga Basin. Fluvial to marginal marine. Time equivalent to Cadna-owie Formation to the north, and Pelican Well Formation to the west.||Unit in Neales River Group.|Includes Trinity Well Sandstone Member in upper part.|Conformably overlies Murta Formation. Is overlain conformably to unconformably by Bulldog Shale.|Quartz sandstone, gritty to gravelly at base; contains exotic lonestones, occasional pebble lenses and carbonaceous clays as basal channel fill; bioturbated and fossiliferous (bivalves, leaves and wood); upper surface calcite cemented or silcreted.|18-NOV-14
14854|Parabarana Sandstone|68713|5|Briefly described|p22|Cretaceous|Cretaceous|||Of the Neales River Group.||||
14854|Parabarana Sandstone|68734|6|Mentioned|p221 Fig.3|Cretaceous|Cretaceous|||||||
14854|Parabarana Sandstone|69019|3|Fully described|p64-65, p85, p87-92, p167.|Cretaceous|Cretaceous|Of Ludbrook (1966); type section ~1 km SE of Parabarana Hill. Composite stratigraphic section in Fig.22. Often associated with ferricrete capping. Fluorite is a pervasive pore filling primary cement, with calcite.||Unit in Neales River Group.||Unconformably overlies Box Bore and Terrapinna Granites. Equivalent to Cadna-owie Formation.|Pale yellowish to pale brown fine-grained quartz sandstone; variably calcite cemented; coarse-grained gritstone lenses; lower zone more silty and dark grey to black from carbonaceous matter; plant fossils abundant.|
14854|Parabarana Sandstone|69023|3|Fully described|p77, p86-88, p93-99, p101, p106, p119|Early Cretaceous|Early Cretaceous|See also p126, p137, p143-144, p151, p159-161, p164, p191-192, p204. Eromanga Basin. Defined by Ludbrook (1966). Type section at Parabarana Hill; detailed profile. Equivalent to Cadna-owie Formation on OODNADATTA map; contrasts between these two units are discussed. Thickness from 3 to ~21m. Tertiary faulting has produced uplift differentials of up to 150m. Overlies Bopeechee Regolith developed on weathered Box Bore and Terrapinna Granites. Is an aquifer, sealed by Bulldog Shale; source for mound springs. Contains calcite and fluorite as pore-filling primary cement. Stratigraphic wells intersection data. Macro-fossils described.|||Includes Trinity Well Sandstone Member.|Unconformably overlies Bopeechee Regolith. Equivalent to Cadna-owie Formation. Is overlain gradationally by Bulldog Shale.|Grey siltstone coarsening upwards to fine- to medium-grained sandstone; sandstone interbeds commonly calcite cemented; a near basal siltstone is commonly carbonaceous; local basal pebbly interval. Local ferricrete capping.|
14854|Parabarana Sandstone|69946|5|Briefly described|p19|||Ludbrook (1966). Crops out on S margin of Eromanga Basin.||||Lateral equivalent of Cadna-owie Formation.||
14854|Parabarana Sandstone|70383|6|Mentioned|p52|||||||Equivalent to Cadna-owie Formation.||
14854|Parabarana Sandstone|70384|5|Briefly described|Map legend.|Aptian|Early Cretaceous|Eromanga Basin. Bioturbated. Fossiliferous: bivalves, leaves, wood. This unit is the rangelands-proximal Basin-wide equivalent to the distal Cadna-owie Formation. Age shown more specifically as Neocomian to Aptian.||of Neales River Group.||Equivalent to Cadna-owie Formation.|Pallid, yellowish, pale grey quartz sandstone, gritty or gravelly at base; exotic lonestones; basal channel infill +/- pebble lenses and trains or carbonaceous clay, local diamictite. Upper 1-2m usually calcite-cemented +/- silcrete +/- ferruginous.|23-JAN-19
14854|Parabarana Sandstone|71342|5|Briefly described|Ch5 p19|||||||Lateral equivalent of the Cadna-owie Formation.||
14854|Parabarana Sandstone|72456|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Marree 1:250k map sheet.  Contains u-shaped burrows and other fossils.|||||Sandstone, calcareous, with clasts of quartz, quartzite and porphyry; sand, gravel and shale.|
14854|Parabarana Sandstone|73251|6|Mentioned|p36|Cretaceous|Cretaceous|Eromanga Basin, Frome Embayment. Marginal thermal maturity.||||Unconformably overlain by Bulldog Shale. Equivalent to Cadna-owie Formation.||
14855|Parachilna Formation|7931|5|Briefly described|p99 Fig. 2|Ediacaran|Ediacaran|Overlies Pound Subgroup (Wilpena Group).||||||07-FEB-11
14855|Parachilna Formation|22646|6|Mentioned|p 102|Early Cambrian|Early Cambrian|Situated in the Adelaide Geosyncline||||||
14855|Parachilna Formation|22766|5|Briefly described|Fig.2 p561, p561||Tommotian|||||||
14855|Parachilna Formation|23211|6|Mentioned|Fig.2|||Of the Hawker Group.||||||22-NOV-06
14855|Parachilna Formation|23287|6|Mentioned|Fig.2-4||Cambrian|In the Adelaide Geosyncline.||||||22-NOV-06
14855|Parachilna Formation|23818|4|Described|p51 Fig.16, p76, p90|Cambrian|Cambrian|Overlain by Wilkawillina Limestone. Underlain by Bunyeroo Formation and Pound Quartzite (both disconformable). Basal unit of the Hawker Group.||||||22-NOV-06
14855|Parachilna Formation|23825|5|Briefly described|p254 Fig.2|Early Cambrian|Early Cambrian|Geological Province: Arrowie Basin.||||||
14855|Parachilna Formation|23981|5|Briefly described|p8-9 Fig. 4, p10 Fig. 5|Tommotian|Tommotian|Overlies Uratanna Formation; conformably overlain by Woodendinna Dolomite; also overlain by Wirrapowie Limestone. Thickness: <570m in Nepabunna Trough. Geological Province: Arrowie Basin. Transgressive succession from lower sandstone to upper siltstone.||||||15-FEB-07
14855|Parachilna Formation|24072|5|Briefly described|p369 Fig.1|Cambrian|Cambrian|Geological Province: Great Artesian Basin.||||||
14855|Parachilna Formation|24138|5|Briefly described|p29|Triassic|Triassic|Light coloured sandstone with abundant worm burrows.||||||
14855|Parachilna Formation|24176|4|Described|p16, p23 Tb. 1|Early Cambrian|Early Cambrian|Argillaceous sandstones, shales, arkosic sandstone.  Max. thickness: 610m.  Geological Province: Mount Painter Province.  See also p27 Tb. 2.||||||
14855|Parachilna Formation|24281|5|Briefly described|p7|Early Cambrian|Early Cambrian|Age: ~560Ma.||||||
14855|Parachilna Formation|24465|5|Briefly described|p345 Fig.2|Early Cambrian|Early Cambrian|Of the Hawker Group.  Geological Province: Arrowie Basin.||||||19-JAN-05
14855|Parachilna Formation|24481|5|Briefly described|p829 Fig. 9|||Overlies the Wilpena Group. Overlain by the Ajax Limestone.||||||
14855|Parachilna Formation|24484|5|Briefly described|p803 Fig. 3|Cambrian|Cambrian|Overlies the Uratanna Formation. Overlain by the Woodendinna Dolomite.||||||
14855|Parachilna Formation|24586|5|Briefly described|p51 Fig. 1, p52 Fig. 3|Early Cambrian|Early Cambrian|Of the Hawker Group (Moralana Supergroup). Geological Province: Adelaide Geosyncline.||||||
14855|Parachilna Formation|29780|4|Described|p47|||||||||
14855|Parachilna Formation|29929|6|Mentioned|Fig.1|||||||||
14855|Parachilna Formation|30051|6|Mentioned|p18|||See also Fig.4||||||
14855|Parachilna Formation|30052|6|Mentioned|p83|||||||||
14855|Parachilna Formation|30174|6|Mentioned|p883|||||||||
14855|Parachilna Formation|30176|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
14855|Parachilna Formation|30220|6|Mentioned|Fig.13|||||||||
14855|Parachilna Formation|30374|6|Mentioned|Fig.5|||Lower Cambrian age. Correlation.||||||
14855|Parachilna Formation|30375|4|Described|p203|||||||||
14855|Parachilna Formation|30516|6|Mentioned|p64|||Lower Cambrian age||||||
14855|Parachilna Formation|30800|6|Mentioned|p220|||See also Fig.1. Cambrian.||||||
14855|Parachilna Formation|30801|6|Mentioned|p5|||Table p5-6. Lower Cambrian age.||||||22-NOV-06
14855|Parachilna Formation|30802|5|Briefly described|p11|||Cambrian age||||||
14855|Parachilna Formation|30807|6|Mentioned|p102|||Suggested map symbol.||||||22-NOV-06
14855|Parachilna Formation|31022|6|Mentioned|Fig. 4|||||||||
14855|Parachilna Formation|31344|5|Briefly described|p2|||See also p3.||||||22-NOV-06
14855|Parachilna Formation|31536|6|Mentioned|p8|||||||||
14855|Parachilna Formation|31539|5|Briefly described|p9|||See also Fig. 8, 9, 17, 24. Cambrian||||||
14855|Parachilna Formation|31541|6|Mentioned|p545|||||||||
14855|Parachilna Formation|31729|4|Described|p110|||Cambrian. See also p113.||||||22-NOV-06
14855|Parachilna Formation|31730|6|Mentioned|p99|||Geochem. Stream sediment sampling.||||||
14855|Parachilna Formation|31797|6|Mentioned|Fig. 2|||L.Cambrian. Of the Hawker Gp.||||||22-NOV-06
14855|Parachilna Formation|32343|6|Mentioned|Table 1|||See also Figs. 3,5.||||||
14855|Parachilna Formation|32504|6|Mentioned|Fig.2|||||||||
14855|Parachilna Formation|32720|6|Mentioned|Table 1|||Of the Hawker Group.||||||22-NOV-06
14855|Parachilna Formation|32722|6|Mentioned|Fig.3|||Stromatolite. L.Cambrian||||||
14855|Parachilna Formation|32724|6|Mentioned|Fig.1|||Marinoan. Correlation||||||
14855|Parachilna Formation|32776|6|Mentioned|Fig.2|||||||||
14855|Parachilna Formation|33035|6|Mentioned|p53|||||||||
14855|Parachilna Formation|33036|6|Mentioned|Fig.2|||||||||
14855|Parachilna Formation|33037|6|Mentioned|Fig.2|||||||||
14855|Parachilna Formation|33474|6|Mentioned|Fig.3|||||||||
14855|Parachilna Formation|33655|4|Described|p97|||||||||
14855|Parachilna Formation|33729|6|Mentioned|p82|||Fauna.||||||
14855|Parachilna Formation|33734|6|Mentioned|p495|||Correlation. Trace fossils.||||||
14855|Parachilna Formation|33932|4|Described|p14|||||||||
14855|Parachilna Formation|33934|4|Described|Fig.2|||L.Camb.||||||
14855|Parachilna Formation|33954|6|Mentioned|p97|||||||||
14855|Parachilna Formation|34122|6|Mentioned|p301|||Lower Cambrian. See also p302.||||||22-NOV-06
14855|Parachilna Formation|34201|6|Mentioned|p369|||Fauna||||||
14855|Parachilna Formation|34202|6|Mentioned|p1058|||Of the Hawker Group.||||||22-NOV-06
14855|Parachilna Formation|34268|6|Mentioned|p260|||||||||
14855|Parachilna Formation|34269|6|Mentioned|Table 1|||||||||
14855|Parachilna Formation|34291|6|Mentioned|p7|||See also pp8,30,31. Cambrian.||||||22-NOV-06
14855|Parachilna Formation|34401|6|Mentioned|p68|||Worm burrows.||||||
14855|Parachilna Formation|34534|6|Mentioned|Fig.2.13|||||||||
14855|Parachilna Formation|34535|6|Mentioned|p78|||See also p79. Cambrian. Fig.16.||||||22-NOV-06
14855|Parachilna Formation|34563|6|Mentioned|p67|||Correlation||||||
14855|Parachilna Formation|34612|5|Briefly described|p90|||Fig.33. Correlation chart. Cambrian||||||
14855|Parachilna Formation|34836|6|Mentioned|p70|||||||||
14855|Parachilna Formation|34959|6|Mentioned|p285|||||||||
14855|Parachilna Formation|35255|6|Mentioned|Fig.6|||||||||
14855|Parachilna Formation|35582|6|Mentioned|Fig.2|||||||||
14855|Parachilna Formation|35798|6|Mentioned|Fig.4|||Correlation of lower units in Desert Syncline drill holes.||||||
14855|Parachilna Formation|36083|5|Briefly described|p472|||||||||
14855|Parachilna Formation|36198|6|Mentioned|Fig.I.2|||||||||
14855|Parachilna Formation|36525|6|Mentioned|Fig.4|||||||||
14855|Parachilna Formation|36622|6|Mentioned|Fig.2|||||||||
14855|Parachilna Formation|37627|6|Mentioned|p186|||||||||
14855|Parachilna Formation|38004|6|Mentioned|p82|||||||||
14855|Parachilna Formation|38068|6|Mentioned|Fig.4|||||||||
14855|Parachilna Formation|38157|6|Mentioned|Table XI|||||||||
14855|Parachilna Formation|38224|4|Described|p396|||||||||
14855|Parachilna Formation|38970|6|Mentioned|p113|||||||||
14855|Parachilna Formation|39131|6|Mentioned|p186|||||||||
14855|Parachilna Formation|39352|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
14855|Parachilna Formation|39675|6|Mentioned|Fig.2|||||||||
14855|Parachilna Formation|40455|6|Mentioned|Fig.2|||||||||
14855|Parachilna Formation|40810|6|Mentioned|p13|||||||||
14855|Parachilna Formation|40852|6|Mentioned|p32|||||||||
14855|Parachilna Formation|40856|5|Briefly described|p312|||||||||
14855|Parachilna Formation|41429|6|Mentioned|p242|||||||||
14855|Parachilna Formation|41457|6|Mentioned|Fig.2|||||||||
14855|Parachilna Formation|41496|5|Briefly described|p52|||||||||
14855|Parachilna Formation|41526|6|Mentioned|p60|||||||||
14855|Parachilna Formation|41801|5|Briefly described|p216|||||||||
14855|Parachilna Formation|42011|5|Briefly described|p457|||||||||
14855|Parachilna Formation|42095|5|Briefly described|Fig.3 P31|||||||||
14855|Parachilna Formation|42192|6|Mentioned|p10|||||||||
14855|Parachilna Formation|42222|6|Mentioned|p20|||||||||
14855|Parachilna Formation|42225|6|Mentioned|p219|||||||||
14855|Parachilna Formation|42242|6|Mentioned|p200|||||||||
14855|Parachilna Formation|42266|6|Mentioned|Fig.2 P292|||||||||
14855|Parachilna Formation|42272|6|Mentioned|Fig.2 P400|||||||||
14855|Parachilna Formation|42433|5|Briefly described|p178|||||||||
14855|Parachilna Formation|42440|6|Mentioned|Fig.2 P602|||||||||
14855|Parachilna Formation|42444|5|Briefly described|Fig.2 P16|||||||||
14855|Parachilna Formation|42458|5|Briefly described|Fig.2 P699|||||||||
14855|Parachilna Formation|43622|6|Mentioned|p38|Early Cambrian||||||||
14855|Parachilna Formation|44133|5|Briefly described|p22|||Disconformably overlies Rawnsley Quartzite. Maximum Thickness: 570m.||||||
14855|Parachilna Formation|44659|5|Briefly described|map legend||Early Cambrian|L.Cambrian, lithology.||||||
14855|Parachilna Formation|44660|14|Not recorded|map legend||Early Cambrian|L.Cambrian.||||||
14855|Parachilna Formation|45102|6|Mentioned|p47|||See also p48,49.||||||22-NOV-06
14855|Parachilna Formation|45155|6|Mentioned|Fig.8|||||||||
14855|Parachilna Formation|60418|5|Briefly described|p135|Early Cambrian|Early Cambrian|Of the Hawker Group. Geological Province: Arrowie Basin of Adelaide Geosyncline.||||||
14855|Parachilna Formation|60889|4|Described|p245-50|Early Cambrian|Early Cambrian|In Flinders Ranges. Thickness: 570 m. Basal sands were probably deposited in lowstand to transgressive tracts; upper part is mainly transgressive coastal to shelf siliciclastics and minor carbonates. Arrowie Basin.|~533 Ma.|Hawker Group||Disconformably overlies Uratanna Formation or where absent, Rawnsley Quartzite. Is overlain by Woodendinna Dolomite and Wirrapowie Limestone.|Upwards-fining sandstones and siltstones with minor carbonates.|21-SEP-17
14855|Parachilna Formation|60959|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of the Hawker Group. Sandstone and siltstone with minor carbonate interbeds.||||||
14855|Parachilna Formation|60990|5|Briefly described|p83 Fig.2 |Atdbanian|Atdbanian|Flinders Ranges.||Hawker Group.||||
14855|Parachilna Formation|61308|5|Briefly described|p7|Cambrian|Cambrian|Shaly sandstone.||||||
14855|Parachilna Formation|61565|5|Briefly described|p609 Fig. 3|Cambrian|Cambrian|Geological Province: Adelaide Fold Belt.||||||
14855|Parachilna Formation|62085|6|Mentioned|p20 fig 5|||||||||
14855|Parachilna Formation|62592|5|Briefly described|p50 Table 5.1, p59.|Early Cambrian|Early Cambrian|Adelaide Geosyncline.||Basal unit in Hawker Group.||Is overlain by Woodendinna Dolomite.|Worm burrow sandstone.|
14855|Parachilna Formation|62783|6|Mentioned|p2 Fig.1|||||||||
14855|Parachilna Formation|63447|5|Briefly described|p962, p963 Fig.2 |Early Cambrian|Early Cambrian|||Hawker Group||||
14855|Parachilna Formation|63569|6|Mentioned|p117 Fig.1|Early Cambrian|Early Cambrian|Arrowie Basin.||||||
14855|Parachilna Formation|64319|5|Briefly described|p354, p355, p356 Fig.2,   |Early Cambrian|Early Cambrian|Hosts the exotic Reaphook zinc phosphate deposit.||||Overlies Wilpena Group. Is overlain by Ajax Limestone.|Consists mainly of sandstone interbedded with siltstone and limestone.|
14855|Parachilna Formation|64455|5|Briefly described|p138 Fig. 1|||Of Hawker Group. White silty sandstone with white sandstone cobbles at the base. Plagiogmus, Diplocraterion.||||||02-MAY-13
14855|Parachilna Formation|64829|5|Briefly described|p1084-5 Figs.1,  2|Early Cambrian|Early Cambrian|Conformably underlies Woodendinna Dolomite; overlies Uratanna Formation in Mt Scott range and Mudlapena Gap. Age is very Early Cambrian. Has intertidal-supratidal palaeosols with trace fossils - pedotype details included.||||||07-FEB-11
14855|Parachilna Formation|65313|6|Mentioned|p577, p576 Fig. 5, p578 Fig. 6|Early Cambrian|Early Cambrian|~200 degrees burial temperature.||Of Hawker Group.||||26-MAR-12
14855|Parachilna Formation|65375|5|Briefly described|p26, p33.|Early Cambrian|Early Cambrian|Arrowie Basin, Flinders Ranges. Trace fossils, Chancelloria spicules and acritarchs in Winulta Formation, Yorke Peninsula, suggest correlation with this unit.||Unit in Hawker Group.||||
14855|Parachilna Formation|65686|5|Briefly described|417, 418, p409 Fig 2|Early Cambrian|Early Cambrian|570m thick. Arrowie Basin.||||Underlies the Woodendinna Dolomite.||07-MAY-12
14855|Parachilna Formation|65892|4|Described|p7 Fig.3, p8, p9 Fig.4, p27, p29 Fig.14 |Early Cambrian|Early Cambrian|See also p33 Fig.18, p35, p39 Fig.21, p41 Fig.23. Arrowie Basin. 570m thick. Abundant worm burrows and first appearance of Skiagia acritarchs.|c.540 Ma.|Unit in Hawker Group.||Overlies Rawnsley Quartzite and Uratanna Formation. Is overlain by Woodendinna Dolomite and Wirrapowie Limestone.|Upwards fining sandstones and siltstones with minor carbonates.|
14855|Parachilna Formation|65925|5|Briefly described|p14 Fig.2.2, Appendix 2.|Early Cambrian|Early Cambrian|Trace fossils include Diplocraterion and Bemella.|||||Upward-fining sandstone with siltstone and minor carbonate interbeds.|
14855|Parachilna Formation|67870|5|Briefly described|p9|Cambrian|Cambrian|Arrowie Basin.||Hawker Group.||||
14855|Parachilna Formation|67907|6|Mentioned|p257|||Mount Scott Range.||||Conformably overlain by Ajax Limestone.|Siliciclastic.|
14855|Parachilna Formation|68030|5|Briefly described|p239,243|Cambrian|Cambrian|Flinders Ranges. Shallow marine, shore-face and lagoonal. Comprises dense accumulations of Diplocraterion burrows and, further up section, diverse trace fossils including Plagiogmus and small helcionellids.||Unit of Hawker Group.||Grades downward into Uratanna Formation. Also underlain by, and onlaps onto Rawnsley Quartzite.||
14855|Parachilna Formation|68735|5|Briefly described|p233, p233 Fig.2, p234, p235 Fig.3|Early Cambrian|Early Cambrian|Arrowie Basin. Shallow marine origin. Basal sandstones often contain the trace fossil Diplocraterion.||Of the Hawker Group.||Disconformably underlain by the Rawnsley Quartzite. Overlain by the Woodendinna Dolomite and the Wirrapowie Limestone.|Comprises a transgressive succession of upward fining sandstones, siltstones, and minor carbonates.|10-APR-17
14855|Parachilna Formation|68993|6|Mentioned|p544 Fig.1|Early Cambrian|Early Cambrian|Arrowie Basin.||Of the Hawker Group.||||
14855|Parachilna Formation|69019|6|Mentioned|p68.|||Considered a distal equivalent of Western Spur Limestone to the N.||||||
14855|Parachilna Formation|69570|5|Briefly described|p421|||Arrowie Syncline, Flinder Ranges. Lowstand to transgressive unit which occurs in the sampled stratigraphic section (Moro).||||Overlain by the Woodendinna Dolomite.|Iron-rich quartz sandstone.|
14855|Parachilna Formation|70833|4|Described|p176,178-179,182-185,188,190,200-201|Terreneuvian|Terreneuvian|Of Arrowie Basin. Key sections: AJX-M and AJX-N (Mount Scott Range); MORO (S of Moro Gorge, Arrowie Syncline), WAR (Warragee Bore, central Flinders Ranges); BALC (Balcoracana Gorge, Bunkers Range); MMT (Bunkers Range, central Flinders Ranges); 10MS-W (Ten Mile South, SE Bunkers Graben). Lowstand to transgressive systems tract. Upper part is heavily bioturbated with abundant Diplocraterion parallelum.||Unit of Hawker Group.||Lowermost unit of Hawker Group. Overlain by Woodendinna Dolostone, or unconformably by Ajax Limestone. Underlain by Uratanna Formation.|Iron-rich, fine- to coarse-grained, cross-bedded, quartz-rich sandstone with thinly bedded siltstone or shale.|
14855|Parachilna Formation|70835|6|Mentioned|p336-337|Cambrian|Cambrian|Arrowie Basin, Flinders Ranges.||||Is overlain by Ajax Limestone or Woodendinna Dolostone.||
14855|Parachilna Formation|71102|5|Briefly described|p252,267|Terreneuvian|Terreneuvian|Of Arrowie Basin.||||Overlain by Woodendinna Dolostone.||
14855|Parachilna Formation|71237|14|Not recorded|p10, 18|||||||||
14855|Parachilna Formation|71238|14|Not recorded|p3, 9-10, 18||Cambrian|||||||
14855|Parachilna Formation|71241|14|Not recorded|p15, 18, p9-10|Cambrian |Cambrian|Includes vertical burrows.||||Disconformably overlies Pound Quartzite. Equivalent to Mount Terrible Formation.||
14855|Parachilna Formation|72449|5|Briefly described|p1, p2 Map Legend|Early Cambrian|Early Cambrian|Includes long vertical and U-shaped burrows. Shown in image on p1, 'Worm burrows in the Parachilna Formation' (photo 042163)||||Underlies Woodendinna Dolomite.|White, fine to coarse-grained, clayey sandstone with shaped burrows, cross-bedding, ripple marks.|
14855|Parachilna Formation|72451|6|Mentioned|p4 Fig. 1|Late Proterozoic|Late Proterozoic|Adelaidean age. Appears only in Figure 1.||||||
14855|Parachilna Formation|73255|6|Mentioned|p534 Fig.2, p542 Fig.10|early Cambrian|early Cambrian|Contains Skolithos linearis and Treptichnus pedum fossils. [Unclear on diagram?]||||Overlies the Uratanna Formation, underlies the Woodendinna Dolomite.||
14860|Paragon Group|6823|6|Mentioned|p203, 205|Palaeoproterozoic|Palaeoproterozoic|||Willyama Supergroup||||26-MAR-22
14860|Paragon Group|22463|6|Mentioned|22 fig 27|Statherian|Statherian|Parent WIllyama Supergroup Geol. province Broken Hill - Olary Domain||||||
14860|Paragon Group|22500|6|Mentioned|p10, 13|||||||||
14860|Paragon Group|22553|5|Briefly described|fig2p77|Proterozoic|Proterozoic|||||||
14860|Paragon Group|22575|6|Mentioned|p179 Fig.2|||in the Broken Hill Block||||||
14860|Paragon Group|22588|6|Mentioned|p85|||||||||
14860|Paragon Group|22631|6|Mentioned|table1, p173|Statherian|Statherian|||||||
14860|Paragon Group|22641|6|Mentioned|p692|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
14860|Paragon Group|22771|5|Briefly described|p44,47-48|||||||||
14860|Paragon Group|22857|4|Described|p45 Tb. 12.2, p388 App1 Tb.A1.1|Paleoproterozoic|Paleoproterozoic|Of the Willyama Supergroup. Max. thickness: ~1700m.||||||07-NOV-08
14860|Paragon Group|22884|5|Briefly described|p40 Fig. 1, p43 Fig. 3, p46|||Of the Willyama Supergroup. Contains Mount Howden Formation. Overlies Sundown Group. Geological province: Olary/Broken Hill Domains.||||||26-MAR-09
14860|Paragon Group|22959|6|Mentioned|p95||Paleoproterozoic|||||||07-NOV-08
14860|Paragon Group|22962|5|Briefly described|p73,76||Statherian|||||||
14860|Paragon Group|22966|5|Briefly described|p2,4||Proterozoic|||||||
14860|Paragon Group|22967|5|Briefly described|p25,6,30,2,3,39,49||Statherian|||||||
14860|Paragon Group|23025|6|Mentioned|Fig1p75|||||||||
14860|Paragon Group|23160|6|Mentioned|fig1|||||||||
14860|Paragon Group|23223|5|Briefly described|p43|||Of the informal Upper Willyama Supergroup. In the Curnamona Province.||||||11-SEP-07
14860|Paragon Group|23248|5|Briefly described|Fig2p169|||||||||
14860|Paragon Group|23346|6|Mentioned|48|||||||||
14860|Paragon Group|23347|6|Mentioned|p51 Tb. 1, p54|||Geological province: Broken Hill Domain. Equivalent to Olary Domain rocks of the Strathearn Group.||||||24-MAR-09
14860|Paragon Group|23369|6|Mentioned|p26|||||||||
14860|Paragon Group|24197|5|Briefly described|p62|||Of the Willyama Supergroup. Organic-rich sediments intially progressing to fine-grained turbidites. Geological Province: Broken Hill Block.||||||07-FEB-11
14860|Paragon Group|24307|4|Described|p974|Proterozoic|Proterozoic|||||||
14860|Paragon Group|38969|4|Described|p210|||||||||
14860|Paragon Group|39662|2|Defined|p433|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
14860|Paragon Group|39883|6|Mentioned|p380|||||||||
14860|Paragon Group|39885|6|Mentioned|Fig.2|||||||||
14860|Paragon Group|40290|6|Mentioned|p5|||||||||
14860|Paragon Group|40595|6|Mentioned|p85|||||||||
14860|Paragon Group|40822|6|Mentioned|Fig.2|||||||||
14860|Paragon Group|41093|4|Described|p253|||||||||
14860|Paragon Group|41145|6|Mentioned|Fig.4|||||||||
14860|Paragon Group|41402|6|Mentioned|p37|||||||||
14860|Paragon Group|41630|5|Briefly described|p3|||||||||
14860|Paragon Group|42261|6|Mentioned|Fig 1 P530|||||||||
14860|Paragon Group|42529|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
14860|Paragon Group|42537|4|Described|p15|||||||||
14860|Paragon Group|42720|5|Briefly described|map legend|Paleoproterozoic||Variation on Paragon Group, NSW.||||||07-NOV-08
14860|Paragon Group|42813|6|Mentioned|p9|||||||||
14860|Paragon Group|42942|6|Mentioned|p17|||of Willyama Supergroup||||||
14860|Paragon Group|42953|6|Mentioned|p59|||||||||
14860|Paragon Group|43052|6|Mentioned|Fig.4.22|||||||||
14860|Paragon Group|43086|6|Mentioned|Fig.3|||||||||
14860|Paragon Group|43263|6|Mentioned|Map Legend||Paleoproterozoic|||||||07-NOV-08
14860|Paragon Group|43265|5|Briefly described|Map Legend||Paleoproterozoic|Of Willyama Supergroup.||||||07-NOV-08
14860|Paragon Group|43266|5|Briefly described|Map Legend||Paleoproterozoic|Of Willyama Supergroup.||||||07-NOV-08
14860|Paragon Group|43269|5|Briefly described|Map Legend||Paleoproterozoic|Of Willyama Supergroup.||||||07-NOV-08
14860|Paragon Group|43572|6|Mentioned|Fig.3.2 p6|||||||||
14860|Paragon Group|43583|5|Briefly described|Table 1, p2138|||||||||
14860|Paragon Group|46598|4|Described|p305|||||||||
14860|Paragon Group|50045|4|Described|p115 Fig. 2, p116 Fig. 3|Statherian|Statherian|Includes Dalnit Bore Metasediments, Bijerkerno Metasediments and Cartwrights Creek Metasediments. Geological Province: Broken Hill Block. Of the Willyama Supergroup. Underlain by Sundown Group. Age: 1640 Ma.||||||26-FEB-13
14860|Paragon Group|50606|5|Briefly described|p1.1|||Of the Willyama Supergroup. Geological Province: Broken Hill Block.||||||
14860|Paragon Group|50619|5|Briefly described|p174 Fig. 1|Paleoproterozoic|Paleoproterozoic|Uppermost unit of the Willyama Supergroup.  Conformably overlies the Sundown Group.  Geological Province: Broken Hill Block.||||||07-NOV-08
14860|Paragon Group|60485|5|Briefly described|p29|||Of the Willyama Supergroup. Geological Province: Broken Hill Domain.||||||
14860|Paragon Group|61262|5|Briefly described|p455 Fig. 11|Paleoproterozoic|Paleoproterozoic|Geological Province: Broken Hill.||||||07-NOV-08
14860|Paragon Group|61606|5|Briefly described|p4 Fig. 2|||Of the Willyama Supergroup. Includes Dalnit Bore Metasediments, Bijerkerno Metasediments, Cartwrights Creek Metasediments.||||||
14860|Paragon Group|61735|5|Briefly described|p635 Fig. 1, p650-51|Paleoproterozoic|Paleoproterozoic|In the Euriowie Block. See also p636 Fig. 2.||||||30-JUN-09
14860|Paragon Group|61736|5|Briefly described|p666 Fig. 3|Paleoproterozoic|Paleoproterozoic|Contains Cartwrights Creek, Bijerkerno and Dalnit Bore Metasediments. Geological province: Broken Hill Domain.||||||
14860|Paragon Group|61936|6|Mentioned|p203|||Geological Province: Curnamona Province.||||||
14860|Paragon Group|62373|5|Briefly described|p503 Fig.2|||Geological Province: Curnamona Province/Broken Hill Domain.||||||
14860|Paragon Group|62473|5|Briefly described|p74|Paleoproterozoic|Paleoproterozoic|Of Willyama Supergroup. Geological province: Broken Hill Domain.||||||17-JUN-09
14860|Paragon Group|62535|5|Briefly described|p663, p665, p666 Fig.3, p668, p671-674|Paleoproterozoic|Paleoproterozoic|Broken Hill district. Ages from the middle of the Group; closely comparable to ages of tuff units associated with the Mount Isa and Hilton Pb-Zn-Ag orebodies (Gun Supersequence). Hosts minor Zn-Pb mineralization.|1657 +/- 4 Ma (middle) - c.1640 Ma (upper).||Cartwrights Creek, Bijerkerno, Dalnit Bore, Metasediments.||Includes tuffaceous sedimentary rocks.|
14860|Paragon Group|62536|4|Described|p633, 635-636, 638, 641, 649-651, 656|||See also p659. Broken Hill area. Similar zircon provenance ages as Broken Hill and Sundown Groups. Contains very minor Pb-Zn mineralisation.|~1655 Ma.||Bijerkerno, Dalnit Bore Metasediments.|Is intruded by Cusin Creek pluton.|Metasedimentary rocks, including calc-silicate and psammitic lithotypes.|
14860|Paragon Group|62592|5|Briefly described|p14, p15, p16 Fig.2.2.|||Broken Hill Domain, Curnamona Province. Coeval with the northern Australian Pb-Zn basins; possibly prospective for Mount Isa and Century styles of mineralisation.|>1650 to <1640 Ma.|Unit in Willyama Supergroup.|Includes King Gunnia Calc-silicate Member; Cartwrights Creek, Bijerkerno and Dalnit Bore Metasediments.|Overlies Sundown Group.||
14860|Paragon Group|62993|6|Mentioned|p35, p37, p39|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain.||Willyama Supergroup|Includes Cartwrights Creek Metasediments, Bijerkerno Metasediments, Dalnit Bore Metasediments|Equivalent to Strathearn Group.||19-DEC-21
14860|Paragon Group|63020|5|Briefly described|p987 Fig. 8|Paleoproterozoic|Paleoproterozoic|Age: ~1657-1640Ma. Geological Province: Curnamona Province (Broken Hill Domain).||||||07-NOV-08
14860|Paragon Group|63102|5|Briefly described|p9,13,35-36,p38-39,59|Neoproterozoic|Neoproterozoic|Geological province: Broken Hill Domain, Curnamona Province.|||Includes Dalnit Bore metasediments, Bijerkerno Metasediments, Cartwight Creek Metasediments and King Ginnia Calc-silicate Member.|||22-OCT-19
14860|Paragon Group|63186|5|Briefly described|p66, p67|Paleoproterozoic|Paleoproterozoic|Of the Willyama Supergroup. Includes Bijerkerno Metasediments. Max. age: ca 1645 Ma. Geological Province: Broken Hill Domain, Curnamona Province.||||||07-NOV-08
14860|Paragon Group|63489|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Includes the Gunnia Calc-Silicate Member. Geological Province: Broken Hill Domain; unnamed equivalents in Olary Domain.||||||07-NOV-08
14860|Paragon Group|63519|5|Briefly described|p5, p10 Fig. 3|Paleoproterozoic|Paleoproterozoic|Includes Cartwrights Creek, Bijerkerno and Dalnit Bore Metasediments. Overlies Sundown Group with sharp contact.||||||07-NOV-08
14860|Paragon Group|63866|5|Briefly described|p36, p38|||Broken Hill Domain, Curnamona Province.||Willyama Supergroup|Includes the Cartwrights Creek Metasediments, Bijerkerno Metasediments and the Dalnit Bore Metasediments.|||
14860|Paragon Group|64097|5|Briefly described|p302, p303|Paleoproterozoic|Paleoproterozoic|Includes Cartwrights Creek, Bijerkerno and Dalnit Bore Metasediments. Overlies Sundown Group. Geological province: Broken Hill Domain/Curnamona Province. Mostly siliciclastic metasediments, tending to be graphitic.||||||07-FEB-11
14860|Paragon Group|64250|6|Mentioned|p25 fig 10|||Broken Hill Province.||Unit in Willyama Supergroup.||||
14860|Paragon Group|64722|5|Briefly described|Fig. 5 p.13|Statherian|Statherian|Broken Hill region, South Australian Craton.||Of Willyama Supergroup.||||11-APR-12
14860|Paragon Group|64725|6|Mentioned|p58 Fig.2. |||||||||
14860|Paragon Group|64741|5|Briefly described|p301 Fig. 4|Paleoproterozoic|Paleoproterozoic|Of Willyama Supergroup. Includes Cartwrights Creek, Bijerkerno and Dalnit Bore Metasediments. Geological province: Broken Hill Domain, Curnamona province. Broadly equivalent to Strathearn Group in the Olary Domain.||||||07-FEB-11
14860|Paragon Group|64742|5|Briefly described|p320, p322, pp326-327, p330, pp332-333.|||Broken Hill Domain. Major and trace element analyses, and Sm-Nd isotope data, are detailed.||Unit in Willyama Supergroup.|Includes King Gunnia Calc-Silicate Member, Cartwrights Creek Metasediments, Bijerkerno Metasediments and Dalnit Bore Metasediments.|||
14860|Paragon Group|64743|5|Briefly described|pp339-340, pp342-344,  pp346-347. |Paleoproterozoic|Paleoproterozoic|Broken Hill Block.|1660-1600 Ma.|Unit in Willyama Supergroup.||Overlies Sundown Group. Equivalent to Mount Howden Subgroup, Olary Block; and to McNamara Group, Mount Isa Inlier.||
14860|Paragon Group|64744|5|Briefly described|p353 Fig.4, p356. |Statherian|Statherian|Broken Hill Domain. Psammopelitic sediments.||Unit in Willyama Supergroup.||||
14860|Paragon Group|64944|5|Briefly described|p28 Fig. 1|Paleoproterozoic|Paleoproterozoic|Of Willyama Supergroup. Geological province: Broken Hill Domain. Equivalent of Strahearn Group in Olary Domain.||||||07-FEB-11
14860|Paragon Group|65887|5|Briefly described|p51|||Primarily pelitic and psammo-pelitic metasediments. Thought to be deposited in a continental slope to deep water environment.||||||
14860|Paragon Group|66302|5|Briefly described|p35, p36 Fig.9, p38, p39, p40, p73|||Broken Hill Domain, Curnamona Province. Represents sag phase deposition post-dating the climax of rifting. Peak metamorphism interpreted to have occurred at 1675 Ma.||Willyama Supergroup|Includes the Cartwrights Creek Metasediments, Bijerkerno Metasediments and the Dalnit Bore Metasediments.|Equivalent to the Strathearn Group.||
14860|Paragon Group|66857|6|Mentioned|p972 Fig.2.|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain.||Unit in Willyama Supergroup.||Overlies Sundown Group.||
14860|Paragon Group|67323|5|Briefly described|Eastern Australia Time-Space Plot, p35|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain, Curnamona Province. Post-rift sedimentation.|~1660-1650 Ma.||Dalnit Bore, Bijerkerno, Cartwright Creek Metasediments.|||
14860|Paragon Group|67621|6|Mentioned|p224|||||||||
14860|Paragon Group|68126|5|Briefly described|p6, p26, p30|||Broken Hill Domain, Curnamona Province.|~1670-1640 Ma (Page et al. in prep).|Willyama Supergroup.||Overlies Sundown Group. Equivalent to Strathearn Group.||
14860|Paragon Group|69999|5|Briefly described|p3, p8 Photos 5,7, p12-13, p15, p20|Paleoproterozoic|Paleoproterozoic|Euriowie Block, Curnamona Province. Upper, post-rift, deeper water, sag phase deposition followed by marine regression. Contains the only greenschist facies rocks from the Olarian Orogeny.|||||Fine-grained chlorite-biotite-chiastolite schist.|
14860|Paragon Group|70000|5|Briefly described|p31, p33-34, p37, p39|Statherian|Statherian|||Unit in Willyama Supergroup.|Includes Cartwrights Creek, Bijerkerno and Dalnit Bore, Metasediments.|Conformably overlies the Sundown Group.|Graphitic siltstones and aluminous metapelitic rocks with minor calc-silicate; grading upwards into albitic, rippled psammitic and interbedded phyllitic rocks; then thinly bedded graphitic, pelitic to psammopelitic phyllite with lesser psammite.|
14860|Paragon Group|70014|5|Briefly described|Map legend|||||Unit in Willyama Supergroup.|Includes Cartwrightrs Creek, Bijerkerno and Dalnit Bore Metasediments.|Overlies Sundown Group.|Mainly graphitic metasediments, including spotted and non-spotted phyllites, chiastolite phyllites and schists, albitic psammites, and very minor calc-silicate rock.|
14860|Paragon Group|70015|5|Briefly described|Map legend|Statherian|Statherian|Mineral deposits (if any) are shown.||Unit in Willyama Supergroup.|Includes Cartwrights Creek, Bijerkerno and Dalnit Bore, Metasediments.|Overlies Sundown Group.|Predominantly graphitic metasedimentary rocks including phyllite, schist, psammite and minor calc-silicate.|
14860|Paragon Group|70405|6|Mentioned|p15, p43 Table 3|Mesoproterozoic|Paleoproterozoic||1640 Ma - 1655 Ma|Wilyama Supergroup||||
14860|Paragon Group|70657|4|Described|p5, p6 Fig.1, p10 Fig.4, p11 Fig.5|Statherian|Statherian|See also p13 Fig.6, p15, p17, p20, p33, p40, p42, p44, p65. Curnamona Province; Broken Hill, Mulyungarie Domains. Unconformity mid-Group ~1655-1651 Ma. Age range inferred from Fig.4.|<1672 +/- 7 Ma - 1642 +/-5 Ma|Upper Willyama Supergroup|Cartwrights Creek, Bijerkerno and Dalnit Bore Metasediments.|Overlies Sundown Group (in Mulyungarie and Broken Hill Domains). Equivalent to the Strathearn Group.||
14860|Paragon Group|70658|5|Briefly described|p2, 7, 15-16|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain, Curnamona Province.|~1655 Ma - 1642 +/- 5 Ma.|Willyama Supergroup.|Cartwrights Creek, Bijerkerno, Dalnit Bore Metasediments.|Equivalent to Strathearn Group (Olary Domain).||
14860|Paragon Group|70858|6|Mentioned|p33|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain, Curnamona Province.||||||
14860|Paragon Group|71968|5|Briefly described|p1,3-4,18,26,28,35-36,38,45-47|Paleoproterozoic|Paleoproterozoic|Geological province: Curnamona province. Occurs at the top of exposed Willyama Supergroup. Depositional age range of c. 1670-1640 Ma (Page et al., 2000; Page et al., 2005a, b; Stevens et al., 2008). Change from sliciclastic-dominated Sundown Group to fine-grained carbonaeous Paragon Group reflect a significant decrease (starving) in siliciclastic sediment input to the Curnamona Rift Basin; also reflects a change from older detrital zircons (c. 1792 Ma) in Sundown Group to younger populations in Paragon Group (c. 1754 Ma), possibly indicating a change in sediment source and supply and possibly exposure of a new source region based on relative sea level change.||Unit of Willyama Supergroup.|Includes Dalnit Bore Metasediments, Bijerkerno Metasediments, Cartwrights Creek Metasediments.|Underlain conformably by Sundown Group.||
14860|Paragon Group|72435|6|Mentioned|p715|Statherian|Statherian|Basal boundary with Sundown Group is gradational in places. Thickness: ~1700 m.|ca 1670 - 1640 Ma|||Underlain by Sundown Group.||
14860|Paragon 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||||
14860|Paragon Group|72461|5|Briefly described|p5-6, p13, p16, p19|||||Willyama Supergroup|Includes the Dalnit Bore Metasediments, Bijerkerno Metasediments and the Cartwrights Creek Metasediments.|Conformably overlies the Sundown Group.|Sedimentary rocks.|
14860|Paragon Group|73165|6|Mentioned|p637, Fig. 12|||Curnamona Province.||||||
14860|Paragon Group|73243|6|Mentioned|p52 Fig.1, p53 Fig.2 p59|Statherian|Statherian|Broken Hill block-Euriowie block.|up to ~1640 Ma|Willyama Supergroup||||
14860|Paragon Group|73308|6|Mentioned|p607, 610, 622||||< c.1640 Ma.|Willyama Supergroup.||||
14860|Paragon Group|73429|6|Mentioned|p106 Fig.2, p107|Statherian|Statherian|Curnamona Province, Broken Hill Domain.||Willyama Supergroup, upper||||
14860|Paragon Group|73482|5|Briefly described|p422 Fig.3, p423, p426-427, p434|||Known thickness of 1.7 km. Younger than 1670 Ma in age. See also p428 Fig.7, p429 Fig.8.||Willyama Supergroup|Cartwright Creek Metasediments, Bijerkerno Metasediments, Dalnit Bore Metasediments|Overlies Sundown Group|Metasediments. Biotite and andalusite metamorphic grades in parts.|
14860|Paragon Group|73512|5|Briefly described|p1-4, p7|Statherian|Statherian|Curnamona Province, Broken Hill Block. Represents deeper-water basin fill. [Also written as upper Paragon Group, p1].||Willyama Supergroup||Underlain by Sundown Group.||
14860|Paragon Group|73524|6|Mentioned|p2|||Sag-phase metasediments.||Willyama Supergroup, upper||||
14860|Paragon Group|73575|5|Briefly described|p828 Fig.2, p829 Fig.3||Statherian|||Willyama Supergroup|Cartwrights Creek Metasediments, Bijerkerno Metasediments, Dalnit Bore Metasediments|Overlies Sundown Group||
14862|Paralana Quartzite|22631|6|Mentioned|p177|||||||||
14862|Paralana Quartzite|22772|4|Described|p64,Table13.1|Cryogenian|Cryogenian|||||||
14862|Paralana Quartzite|22857|5|Briefly described|p64, Tb. 13.1 (insert p70-71)|Willouran|Willouran|Of the Arkaroola Subgroup (Callanna Group). See also p403 App.1 Tb.A1.3.||||||16-JAN-08
14862|Paralana Quartzite|23314|5|Briefly described|331 Fig.2|||||||||
14862|Paralana Quartzite|23394|5|Briefly described|Map legend|Proterozoic|Proterozoic|||||||
14862|Paralana Quartzite|23411|6|Mentioned|Map Legend|||||||||
14862|Paralana Quartzite|23818|5|Briefly described|p50|||Max. thickness: 4000 ft.||||||
14862|Paralana Quartzite|24176|4|Described|p9, p26 Tb. 1|Adelaidean|Adelaidean|Of the Callanna Beds.  Pink quartzites, grey sandstones; minor actinolitic quartzites and amphibolites. Age is Willouran. Overlain and intertongued by Wywyana Formation. Max. thickness: 1220m. Geological Province: Mount Painter Province.||||||25-JAN-08
14862|Paralana Quartzite|24546|5|Briefly described|p2 - 3 Fig.2|Neoproterozoic|Neoproterozoic|Of Arkaroola Subgroup. Geological Province: Adelaide Fold Belt.||||||16-JAN-08
14862|Paralana Quartzite|24593|5|Briefly described|p612 Fig. 1a|Adelaidean|Adelaidean|Of the Callana Group. Geological Province: Mount Painter Inlier. See also p613 Fig. 1b.||||||25-JAN-08
14862|Paralana Quartzite|30176|6|Mentioned|Map legend|Adelaidean|Adelaidean|Willouran||||||
14862|Paralana Quartzite|30177|2|Defined|p126|Adelaidean|Adelaidean|See also p49. Type section: North and south of East Painter Creek, lat. 30degrees 14'27"S  long.139degrees25'24"E to lat. 30degrees 15'02" S long. 139degrees25'00" E to lat. 30degrees 15'31"S  long. 139degrees24'38"E.||||||25-NOV-22
14862|Paralana Quartzite|30261|6|Mentioned|Table 1|||Willouran age.||||||30-AUG-18
14862|Paralana Quartzite|30511|6|Mentioned|p36|||||||||
14862|Paralana Quartzite|30712|5|Briefly described|p.56.|||||||||
14862|Paralana Quartzite|30801|6|Mentioned|p5|||Lower Callanna Beds. Table p5-6.||||||30-AUG-18
14862|Paralana Quartzite|32724|6|Mentioned|Fig.1|||Willouran. Correlation||||||
14862|Paralana Quartzite|33474|6|Mentioned|Fig.4|||||||||
14862|Paralana Quartzite|34269|6|Mentioned|Table 1|||||||||
14862|Paralana Quartzite|34535|5|Briefly described|Fig.16|||Willouran||||||
14862|Paralana Quartzite|34812|6|Mentioned|p134|||See also Table 8.||||||
14862|Paralana Quartzite|35255|6|Mentioned|p11|||||||||
14862|Paralana Quartzite|35270|6|Mentioned|Fig.3|||||||||
14862|Paralana Quartzite|36733|6|Mentioned|Table 5|||||||||
14862|Paralana Quartzite|36873|5|Briefly described|p27|||||||||
14862|Paralana Quartzite|37372|6|Mentioned|p2|||||||||
14862|Paralana Quartzite|37461|4|Described|p335|||See also Table 5.I.||||||20-FEB-08
14862|Paralana Quartzite|37854|6|Mentioned|p8|||||||||
14862|Paralana Quartzite|38068|6|Mentioned|Fig.4|||||||||
14862|Paralana Quartzite|38157|6|Mentioned|Table II|||||||||
14862|Paralana Quartzite|39348|6|Mentioned|Map legend|Adelaidean|Adelaidean|Willouran||||||
14862|Paralana Quartzite|39352|6|Mentioned|Map legend|Adelaidean|Adelaidean|Willouran||||||
14862|Paralana Quartzite|39404|6|Mentioned|Map legend|Adelaidean|Adelaidean|Willouran||||||
14862|Paralana Quartzite|40294|6|Mentioned|Table 1|||See also Table 2||||||
14862|Paralana Quartzite|41401|6|Mentioned|p31|||||||||
14862|Paralana Quartzite|41403|3|Fully described|p44|||See also Table 5.||||||20-FEB-08
14862|Paralana Quartzite|41405|6|Mentioned|p131|||||||||
14862|Paralana Quartzite|42098|5|Briefly described|Table 2 P54|||||||||
14862|Paralana Quartzite|42222|5|Briefly described|p11|||||||||
14862|Paralana Quartzite|42223|6|Mentioned|p46|||||||||
14862|Paralana Quartzite|42357|6|Mentioned|p8|||||||||
14862|Paralana Quartzite|42624|6|Mentioned|p20|||||||||
14862|Paralana Quartzite|43052|5|Briefly described|p172|||Of the Arkaroola Subgroup.||||||20-FEB-08
14862|Paralana Quartzite|44111|6|Mentioned|p.58 Fig. 2|||in Adelaide Geosyncline, presented as "Paralana" only in Fig. 2.||||||
14862|Paralana Quartzite|60718|5|Briefly described|p49|Adelaidean|Adelaidean|Braided, fluvial to shallow marine facies. Thickness: ~1000m.||Of Arkaroola Subgroup, Mount Painter Inlier.||Underlies Wywyana Formation.||15-APR-11
14862|Paralana Quartzite|61556|14|Not recorded|p10|Willouran|Willouran|||||||
14862|Paralana Quartzite|62592|5|Briefly described|p50 Table 5.1, p57.|Willouran|Willouran|Adelaide Geosyncline. Start of deposition; a highly mature quartzose sandstone, overlying Mesoproterozoic granite or felsic volcanics and quartzites with only a slight angular unconformity, making seismic distinction difficult.|c.830 Ma.|Basal unit in Arkaroola Subgroup.||Is overlain gradationally by Wywyana Formation.|Orthoquartzite.|
14862|Paralana Quartzite|62724|5|Briefly described|p16|Willouran|Willouran|Of the Callana Group. Comprises mature quartz sandstone. In northern Flinders Ranges - mature quartz sandstones of the Adelaide Geosyncline.||||||07-FEB-11
14862|Paralana Quartzite|62993|5|Briefly described|p30|Neoproterozoic|Neoproterozoic|||Arkaroola Subgroup|||Clean quartzites.|17-DEC-21
14862|Paralana Quartzite|64793|6|Mentioned|p285 fig 4|||Adelaide Rift Complex.||Unit in Callanna Group.||||
14862|Paralana Quartzite|65338|6|Mentioned|p59.|||||Unit in Arkaroola Subgroup.|Includes Shanahan Conglomerate Member.|||
14862|Paralana Quartzite|65892|6|Mentioned|p40.|Neoproterozoic|Neoproterozoic|||||||
14862|Paralana Quartzite|65925|5|Briefly described|p124 Fig.3, p128.|||||Unit in Callanna Group.|||Quartzite, minor conglomerate.|
14862|Paralana Quartzite|68068|5|Briefly described|Map legend|Willouran|Willouran|Adelaide Geosyncline.||Unit in Arkaroola Subgroup.|Includes Shanahan Conglomerate Member.||Basal conglomerate (Member); massive to poorly-bedded orthoquartzite, heavy-mineral bands near base.|
14862|Paralana Quartzite|69023|3|Fully described|p27, p61-64, p146|Neoproterozoic|Neoproterozoic|Exposed at Prospect Hill. Basal to Adelaide Geosyncline sequence. Thickness over 90m.|>830 Ma.|Unit in Arkaroola Subgroup.|Includes Shanahan Conglomerate Member.|Unconformably overlies Petermorra Volcanics.|Basal pebble and cobble conglomerate bands; hard pale bluish-grey siliceous and cross-bedded quartzite.|
14862|Paralana Quartzite|70384|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Adelaide Geosyncline. The base rests on a major unconformity surface.||Arkaroola Subgroup.|Shanahan Conglomerate Member.|Is overlain conformably by Wywyana Formation.|Massive to poorly-bedded orthoquartzite, heavy mineral bands near base.|
14862|Paralana Quartzite|73222|6|Mentioned|p7|Tonian|Tonian|Adelaide Rift Complex, Gammon Ranges. Willouran.||Arkaroola Subgroup, Callanna Group, Warrina Supergroup||Underlain by [?]Shanahan Conglomerate Member. Overlain by Wywyana Formation.||
14862|Paralana Quartzite|74367|5|Briefly described|p7 Fig.6, p8-9, p12-14, p16, p20|Tonian|Tonian|Restricted to the Arkaroola area.|1177+/-28 Ma LA-ICP-MS detrital zircon MDA|Arkaroola Subgroup||||
14866|Parara Limestone|22643|5|Briefly described|p191, fig3,6|Early Cambrian|Early Cambrian|||||||
14866|Parara Limestone|22766|5|Briefly described|Fig.2 p561|Early Cambrian|Early Cambrian|||||||
14866|Parara Limestone|23818|5|Briefly described|p87 Fig.33, p90|Cambrian|Cambrian|Of the Hawker Group. Interfingers with the Wilkawillina Limestone, Bunkers Sandstone and Oraparinna Shale.||||||
14866|Parara Limestone|23827|5|Briefly described|p259|Cambrian|Cambrian|||||||
14866|Parara Limestone|23981|5|Briefly described|p8-9 Fig. 4, p21|Early Cambrian|Early Cambrian|Conformably overlies Kulpara Formation; underlies Minlaton Formation. Max. thickness: 270m; only 25m at type section. Geological Province: Stansbury Basin. (Yorke Peninsula). Different lithologies are given for different parts of the basin.||||||04-FEB-08
14866|Parara Limestone|24176|4|Described|p17, p23 Tb. 1|Cambrian|Cambrian|Dark grey shaly limestone.  Intertongued by the Wilkawillina Limestone.  Geological Province: Mount Painter Province.||||||
14866|Parara Limestone|24360|5|Briefly described|p53|Cambrian|Cambrian|Geological Province: Yorke Peninsula, Gawler Craton||||||
14866|Parara Limestone|24465|5|Briefly described|p345 Fig.2|Early Cambrian|Early Cambrian|Contains the Koolywurtie Member.  Geological Province: Stansbury Basin.||||||19-JAN-05
14866|Parara Limestone|29780|4|Described|p107|||||||||
14866|Parara Limestone|29832|6|Mentioned|p123|||||||||
14866|Parara Limestone|29833|6|Mentioned|p142|||||||||
14866|Parara Limestone|29841|4|Described|p103|||||||||
14866|Parara Limestone|29842|4|Described|p123|||||||||
14866|Parara Limestone|29929|6|Mentioned|p225|||||||||
14866|Parara Limestone|30051|6|Mentioned|p25|||||||||
14866|Parara Limestone|30052|6|Mentioned|p25|||||||||
14866|Parara Limestone|30176|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
14866|Parara Limestone|30198|6|Mentioned|p96|||Refers to aquifers and lithology on Table 2||||||
14866|Parara Limestone|30220|6|Mentioned|Fig.13|||||||||
14866|Parara Limestone|30374|6|Mentioned|Fig.5|||Lower Cambrian age. Correlation.||||||
14866|Parara Limestone|30377|6|Mentioned|p203|||||||||
14866|Parara Limestone|30801|6|Mentioned|p5|||Lower Cambrian. Table P5-6||||||
14866|Parara Limestone|30802|5|Briefly described|p11|||Cambrian age||||||
14866|Parara Limestone|30807|6|Mentioned|p102|||Suggested map symbol||||||
14866|Parara Limestone|31539|6|Mentioned|Fig. 8|||See also Fig. 11, 17, 25, 28. Cambrian||||||
14866|Parara Limestone|31706|6|Mentioned|p633|||Cambrian correlation chart||||||
14866|Parara Limestone|31730|6|Mentioned|p99|||Geochem. Stream sediment sampling.||||||
14866|Parara Limestone|31797|6|Mentioned|Fig. 2|||L.Cambrian. Hawker Gp.||||||
14866|Parara Limestone|32720|6|Mentioned|Table 1|||Hawker Gp.||||||
14866|Parara Limestone|32722|6|Mentioned|Fig.3|||Stromatolite||||||
14866|Parara Limestone|33210|4|Described|p110|||Hydrology discussed||||||
14866|Parara Limestone|33332|4|Described|p10|||See also pp11,12,14 and 15. Lower Cambrian.||||||02-JUL-08
14866|Parara Limestone|33471|6|Mentioned|Fig.1|||||||||
14866|Parara Limestone|33474|6|Mentioned|Fig.3|||||||||
14866|Parara Limestone|33932|4|Described|p17|||||||||
14866|Parara Limestone|33934|4|Described|Fig.2|||Lower Cambrian.||||||02-JUL-08
14866|Parara Limestone|33972|6|Mentioned|Fig.2|||||||||
14866|Parara Limestone|33973|6|Mentioned|p18|||||||||
14866|Parara Limestone|34269|6|Mentioned|Table 1|||||||||
14866|Parara Limestone|34536|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
14866|Parara Limestone|34612|4|Described|p91|||Fig.33. Correlation chart. Cambrian||||||
14866|Parara Limestone|34615|6|Mentioned|p7|||Shown on Figure.||||||
14866|Parara Limestone|34835|6|Mentioned|p27|||||||||
14866|Parara Limestone|35051|5|Briefly described|p203|||||||||
14866|Parara Limestone|35075|6|Mentioned|p77|||||||||
14866|Parara Limestone|35255|6|Mentioned|Fig.8|||||||||
14866|Parara Limestone|35373|6|Mentioned|p12|||||||||
14866|Parara Limestone|35395|6|Mentioned|p105|||||||||
14866|Parara Limestone|35577|6|Mentioned|p12|||||||||
14866|Parara Limestone|36198|6|Mentioned|Fig.I.2|||||||||
14866|Parara Limestone|36525|6|Mentioned|Fig.4|||See also Fig.5.||||||
14866|Parara Limestone|36746|6|Mentioned|p85|||||||||
14866|Parara Limestone|38068|6|Mentioned|p69|||||||||
14866|Parara Limestone|39806|6|Mentioned|p210|||||||||
14866|Parara Limestone|40003|5|Briefly described|Table 12|||||||||
14866|Parara Limestone|40217|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
14866|Parara Limestone|40431|6|Mentioned|p12|||||||||
14866|Parara Limestone|40455|5|Briefly described|p71|||Also mention on Fig.2.||||||
14866|Parara Limestone|40672|4|Described|p2|||||||||
14866|Parara Limestone|40831|6|Mentioned|p5|||||||||
14866|Parara Limestone|40856|6|Mentioned|Fig.23.6|||||||||
14866|Parara Limestone|40914|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
14866|Parara Limestone|41104|6|Mentioned|p246|||||||||
14866|Parara Limestone|41107|5|Briefly described|p179|||||||||
14866|Parara Limestone|41457|6|Mentioned|p3|||||||||
14866|Parara Limestone|41496|5|Briefly described|p52|||||||||
14866|Parara Limestone|41526|6|Mentioned|p61|||||||||
14866|Parara Limestone|41853|6|Mentioned|p198|||||||||
14866|Parara Limestone|41996|6|Mentioned|p2|||||||||
14866|Parara Limestone|42011|6|Mentioned|p459|||||||||
14866|Parara Limestone|42192|6|Mentioned|p1|||||||||
14866|Parara Limestone|42213|4|Described|p471|||See also Fig.2||||||
14866|Parara Limestone|42222|5|Briefly described|p20|||||||||
14866|Parara Limestone|42225|4|Described|p221|||||||||
14866|Parara Limestone|42226|4|Described|p231|||||||||
14866|Parara Limestone|42232|5|Briefly described|p284|||||||||
14866|Parara Limestone|42233|6|Mentioned|p259|||||||||
14866|Parara Limestone|42266|6|Mentioned|p299|||||||||
14866|Parara Limestone|42269|6|Mentioned|Fig.1 P335|||||||||
14866|Parara Limestone|42270|6|Mentioned|p363|||||||||
14866|Parara Limestone|42272|6|Mentioned|p413|||||||||
14866|Parara Limestone|42440|6|Mentioned|Fig.2 P602|||||||||
14866|Parara Limestone|42444|5|Briefly described|Fig.2 P16|||||||||
14866|Parara Limestone|42458|5|Briefly described|Fig.2 P699|||||||||
14866|Parara Limestone|42488|5|Briefly described|p185, Fig.2 p187|||||||||
14866|Parara Limestone|42573|5|Briefly described|Fig.1 P190|||||||||
14866|Parara Limestone|42731|5|Briefly described|map legend|Early Cambrian||||||||
14866|Parara Limestone|43052|5|Briefly described|Table 2.1|||||||||
14866|Parara Limestone|43053|5|Briefly described|Map Legend|Cambrian|Cambrian|Marine shelf to basinal carbonate, minor basal sandstone.||||||25-MAY-05
14866|Parara Limestone|43258|5|Briefly described|Map Legend||Cambrian|||||||
14866|Parara Limestone|43298|6|Mentioned|Map Legend||Cambrian|||||||
14866|Parara Limestone|43759|6|Mentioned|p451|||||||||
14866|Parara Limestone|43845|6|Mentioned|Fig4 p44|||||||||12-JUL-16
14866|Parara Limestone|44040|14|Not recorded|p37,38|||||||||
14866|Parara Limestone|44133|5|Briefly described|p3, 6, 8, 4 Fig. 7.2, 10|Botomian|Atdabanian|Conformably overlies Kulpara Formation. Geological Province: Stansbury Basin. Maximum Thickness: 270m.||||||
14866|Parara Limestone|44659|5|Briefly described|map legend||Early Cambrian|L.Cambrian, lithology.||||||
14866|Parara Limestone|44660|14|Not recorded|map legend||Early Cambrian|L.Cambrian.||||||
14866|Parara Limestone|44691|4|Described|map legend||Early Cambrian|(I/53-12). Lower Cambrian.||||||
14866|Parara Limestone|45102|6|Mentioned|p37|||See also P41,47,48||||||
14866|Parara Limestone|48971|6|Mentioned|p9|||See also P18,20.||||||
14866|Parara Limestone|60264|6|Mentioned|p579|Early Cambrian|Early Cambrian|In the Yorke Peninsula area.||||||
14866|Parara Limestone|60418|5|Briefly described|p135|||Shallow water facies. Geological Province: Stansbury Basin.||||||18-MAY-05
14866|Parara Limestone|60419|5|Briefly described|p37|Early Cambrian|Early Cambrian|||||||
14866|Parara Limestone|60953|5|Briefly described|Map Legend|Cambrian|Cambrian|Geological Province: Spencer Shelf.||||||
14866|Parara Limestone|60958|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Nodular limestone with minor mottles argillaceous limestone and thin calcareous shale. Geological Province: Stansbury Basin.||||||14-APR-05
14866|Parara Limestone|60990|5|Briefly described|p83, p85|||Yorke Peninsula, Stansbury Basin. Faunal links with Antarctica.|||Koolywurtie Member.|||
14866|Parara Limestone|61108|5|Briefly described|map legend|Cambrian|Cambrian|Marine shelf to basinal carbonate. Geological Province: Spencer Shelf.||||||06-JUN-05
14866|Parara Limestone|61121|5|Briefly described|Map legend|Early Cambrian|Early Cambrian|Contains the Koolywurtie Limestone Member. Nodular limestone with minor mottled argillaceous limestone and thin calcareous shale. Age is Late Atdabanian to Botoman. Geological Province: Stansbury Basin.||||||14-MAR-12
14866|Parara Limestone|62784|6|Mentioned|p28|Cambrian|Cambrian|Single, poorly preserved specimen of Indianidae gen. et sp. indet. C from this unit was described by Bengston et al. (1990).||||||
14866|Parara Limestone|62790|5|Briefly described|p206, p207|Early Cambrian|Early Cambrian|Atdabanian age, occurs at Curramulka Quarry, Yorke Peninsula. The first report of bradoriids, and oldest known record of the group in Australia, is from this unit. Includes species belonging to the Hipponicharionidae and Monasteriidae, with trilobites.||||||
14866|Parara Limestone|63447|5|Briefly described|p961,p963 Fig.2 |Early Cambrian|Early Cambrian|Shown in brackets as ?equivalent to Mernmerna Formation||?Hawker Group||Equivalent to the Mernmerna Formation.||
14866|Parara Limestone|63569|5|Briefly described|pp121-123, p129, p131, 138|Early Cambrian|Early Cambrian|Contains trilobite taxa from the Abadiella huoi Zone.||||||
14866|Parara Limestone|64282|5|Briefly described|Map legend|Early Cambrian|Early Cambrian|Nodular limestone with minor mottled argillaceous limestone and thin calcareous shale; Archaeocyaths, trilobites and acritarchs.||||||02-JUL-08
14866|Parara Limestone|65375|4|Described|p27 Fig.5, p28 Fig.6, p55.|Cambrian|Cambrian|Contains Yorkella, Pararaia and Redlichia trilobites and abundant acritarchs. Quarried at Curramulka for roadworks. Contains only minor galena, sphalerite and chalcopyrite mineralisation. Possible hydrocarbon source rock (TOC mean = 0.3%).|||Includes Koolywurtie Limestone Member.|Overlies Kulpara Formation. Is unconformably overlain by Minlaton Formation.|Nodular limestone with minor mottled argillaceous limestone and calcareous shale.|
14866|Parara Limestone|65376|6|Mentioned|p92 Fig. 2.82. |Cambrian|Cambrian|||||||
14866|Parara Limestone|65625|5|Briefly described|p103 Fig.2|Early Cambrian|Early Cambrian|Ardrossan - Curramulka, Lake Frome areas.||||Overlies Kulpara Limestone, Wilkawillina Limestone. Underlies Bunkers Sandstone.||18-FEB-11
14866|Parara Limestone|65686|6|Mentioned|p412, 413, 415 Fig 4|||Yorke Peninsula.||||||
14866|Parara Limestone|65892|5|Briefly described|p9 Fig.4, p24, p29 Fig.14. |Early Cambrian|Early Cambrian|Yorke Peninsula. Contains trilobites and small shelly fossils.|||Includes Koolywurtie Limestone Member.|Overlies Kulpara Formation. Is overlain by Minlaton Formation.|Siltstone, pale grey limestone.|
14866|Parara Limestone|65925|5|Briefly described|Appendix 2.||||||||Algal and dolomitic limestone; glauconitic sandstone interbeds.|
14866|Parara Limestone|66761|5|Briefly described|p244-246, 254-255|Cambrian|Cambrian|55 m interval in PIRSA stratigraphic hole Investigator 1. Underlies the Smith Bay Shale? but contact may be faulted. Better known from Yorke Peninsula.||||Overlies the Kulpara Formation.||14-MAR-12
14866|Parara Limestone|67344|6|Mentioned|p264 Tb.3|Cambrian|Cambrian|Of the Stansbury Basin. Cambrian series 2 age.||||||
14866|Parara Limestone|67536|6|Mentioned|Map Legend||||||||Marine shelf to basinal carbonate, minor basal sandstone.|
14866|Parara Limestone|68735|6|Mentioned|p233 Fig.2, p235 Fig.3|Early Cambrian|Early Cambrian|Stansbury Basin.|||Koolywurtie Member.||Carbonate-dominated.|10-APR-17
14866|Parara Limestone|68993|6|Mentioned|p544 Fig.1|Early Cambrian|Early Cambrian|Yorke Peninsula.|||Includes the Koolywurtie Member.|||
14866|Parara Limestone|70833|5|Briefly described|p200,202-203|Cambrian|Cambrian|Of Western Stansbury Basin. Includes D. odyssei zone. Time equivalent to Heatherdale Shale and approximately equivalent to the Mernmerna Formation.|||Includes Koolywurtie Member.|Overlain unconformably by Minlaton Formation. Underlain unconformably by Kulpara Limestone.||08-AUG-19
14866|Parara Limestone|70835|6|Mentioned|p337, 350, 354|Cambrian|Cambrian|Yorke Peninsula. Lower Cambrian. Mentioned in connection with macromollusc fossils held in the South Australian Museum.||||Equivalent to Mernmerna Formation.||
14866|Parara Limestone|71102|5|Briefly described|p249,254,258,260|||Of Arrowie and Stansbury basins. Equivalent to Mernmerna Formation. Fossil assemblage described.|||Includes Koolywurtie Limestone Member.|||05-SEP-19
14866|Parara Limestone|73092|6|Mentioned|p2|Cambrian|Neoproterozoic|||||||
14866|Parara Limestone|73107|5|Briefly described|Map legend.|Early Cambrian|Early Cambrian|Stansbury Basin. Archaeocyaths, trilobites Yorkella australis, Pararaia and acritarchs. Subsurface only.|||||Nodular limestone with minor mottled argillaceous limestone and thin calcareous shale.|
14866|Parara Limestone|73247|6|Mentioned|p205, p207|Cambrian (Stage 4)|Cambrian (Stage 2)|Yorke Peninsula. [Also written as ""Parara Limestone"" in the Kangaroo Island Investigator 1 Big Gully section; inferred to indicate tentative correlation].",,|||Koolywurtie Limestone Member|Unconformably underlain by Kulpara Formation. Unconformably overlain by Minlaton Formation. Equivalent to Mount McDonnell Formation.||03-FEB-23
14873|Parilla Sand|2967|4|Described|p9, 12, p15 Fig.2.2, p18, 21-22, 24|Pliocene|Miocene|Murray Basin. Is shown as a unit in the Murray Group in Fig.2.2, but on p24 is said to have been excluded from that Group by Lawrence (1966). A 60-100m thick unconfined aquifer of marine origin; saline. Late Tertiary. Originally defined by Firman (1965) in South Australia; Lawrence (1975) included the Victorian equivalents of the marine Loxton Sand of South Australia. Is separated from the overlying Blanchetown Clay by the Karoonda Surface. Hydrochemistry (salinity) detailed. See also p26-29, 31-33, 35-37, 40-41, 43-52, 80, 84-85, 87-88, 96, 102, 118, 132, 142, 145, 148, 154-156, 158, 162, 169, 172-179, 181-185, 187, 191-193, 195, 197-198, 205, 208-209, 213, 216, 221, 224, 229, 231, 235, 247, 254, 257, 259, 278, 280, 283, 285-286, 290, 292, 295-297, 300, 304, 313, 315, 318-320, 322, 328, 331, 333-334, 336-338.||Murray Group.|Kerang Sand Member, Tragowel Member, Wandella Sandstone Member.|Overlies Bookpurnong beds and Calivil Formation. Is separated from the underlying Geera Clay by the Mologa Surface. Is overlain by Shepparton Formation. See COMMENTS for more.|Sparingly fossiliferous, fine-grained, transgressive marine sandstones. Weathering has produced a silicified and ferruginised capping (the Karoonda Surface). Local occurrences of heavy mineral sands (beach or shallow marine placers) up to 1m thick.|
14873|Parilla Sand|10010|5|Briefly described|p12 Fig. 3|Late Pliocene|Late Pliocene|Geological Province: Murray Basin.||||||13-AUG-07
14873|Parilla Sand|22531|6|Mentioned|p2|Pliocene|Pliocene|||||||
14873|Parilla Sand|22756|6|Mentioned|P31|||||||||
14873|Parilla Sand|22773|5|Briefly described|Fig24.8p352,354||Pliocene|||||||
14873|Parilla Sand|22782|5|Briefly described|p13|Pliocene|Pliocene|||||||
14873|Parilla Sand|22799|4|Described|p35|||||||||
14873|Parilla Sand|22857|5|Briefly described|p339, p352 Fig. 24.8, p354|Late Pliocene|Late Pliocene|Marginal marine to non-marine sands. Heavy mineral sands containing rutile, zircon and ilmenite. Geological Province: Murray Basin.||||||
14873|Parilla Sand|22887|5|Briefly described|Fig.6 p13|Late Pliocene||||||||
14873|Parilla Sand|22893|3|Fully described|p34,35,37 fig9,11|Pleistocene|Pliocene|||||||
14873|Parilla Sand|23164|4|Described|p16|Early Pliocene|Late Miocene|||||||
14873|Parilla Sand|23166|5|Briefly described|Map legend||Miocene|||||||
14873|Parilla Sand|23167|5|Briefly described|Map legend||Miocene|||||||
14873|Parilla Sand|23168|5|Briefly described|Map legend||Miocene|||||||
14873|Parilla Sand|23169|5|Briefly described|Map legend||Miocene|||||||
14873|Parilla Sand|23307|5|Briefly described|Map Legend|Neogene|Neogene|||||||
14873|Parilla Sand|23560|5|Briefly described|p152|Pliocene|Pliocene|||||||
14873|Parilla Sand|23603|5|Briefly described|p11|Early Pliocene|Late Miocene|||||||
14873|Parilla Sand|23604|5|Briefly described|Map Legend|Tertiary|Tertiary|||||||
14873|Parilla Sand|23605|5|Briefly described|Map Legend|Tertiary|Tertiary|||||||
14873|Parilla Sand|23606|5|Briefly described|Map Legend|Tertiary|Tertiary|||||||
14873|Parilla Sand|23607|5|Briefly described|Map Legend|Tertiary|Tertiary|||||||
14873|Parilla Sand|23818|5|Briefly described|p174 Fig.84, p213|Pliocene|Pliocene|Geological Province: Murray Basin. Overlying unit: Coomandook Formation.||||||
14873|Parilla Sand|23884|5|Briefly described|p155 Fig.13.2|Late Pliocene|Late Pliocene|Geological Province: Murray Basin. See also Parilla Sands.||||||28-APR-05
14873|Parilla Sand|24104|5|Briefly described|p149|Neogene|Neogene|Geological Province: Murray Basin.||||||
14873|Parilla Sand|24177|3|Fully described|p72, p103|Early Pliocene|Late Miocene|Overlain by the Shepparton Formation. Interfingered with Calivil Formation. Indication that the Bagshot Formation of Bendigo region (Cherry & Wilkinson) belongs to Parilla Sand due to no lithological differences. Geological Province: Murray Basin.||||||
14873|Parilla Sand|24328|5|Briefly described|Map legend|Neogene|Neogene|||||||
14873|Parilla Sand|24329|5|Briefly described|Map legend|Neogene|Neogene|||||||
14873|Parilla Sand|24439|5|Briefly described|p8, p15|Pliocene|Pliocene|Siliceous marine deposits.  Of Brown and Wilkinson (1991).  See also p47 Fig. 22.  Geological Province: Murray Basin.||||||06-APR-05
14873|Parilla Sand|24440|5|Briefly described|Map legend|||||||||
14873|Parilla Sand|24468|6|Mentioned|p415|Pliocene|Pliocene|Geological Province: Gippsland Basin||||||
14873|Parilla Sand|24551|5|Briefly described|p322 Fig. 10.29, p324, 306|||Of the Wunghnu Group.  Geological Province: Murray Basin.  Max thickness: 150m.||||||
14873|Parilla Sand|24574|6|Mentioned|p705|||Geological Province: Murray Basin||||||
14873|Parilla Sand|29591|6|Mentioned|Table 20|||||||||
14873|Parilla Sand|29697|5|Briefly described|Table 1|||||||||
14873|Parilla Sand|29898|6|Mentioned|p138|||||||||
14873|Parilla Sand|30145|6|Mentioned|p183|||||||||
14873|Parilla Sand|30522|6|Mentioned|Map legend|Pliocene|Pliocene|||||||
14873|Parilla Sand|30581|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
14873|Parilla Sand|30750|6|Mentioned|p1|||Late Pliocene||||||
14873|Parilla Sand|30751|6|Mentioned|Map legend|late Pliocene|late Pliocene|||||||
14873|Parilla Sand|30752|6|Mentioned|p4|||||||||
14873|Parilla Sand|30753|4|Described|p16|||Upper Pliocene||||||
14873|Parilla Sand|30754|2|Defined|Appendix 1|late Pliocene|late Pliocene|See also p14,22-24,38,41.||||||10-NOV-10
14873|Parilla Sand|30758|6|Mentioned|p66|||Stratigraphy||||||
14873|Parilla Sand|30807|6|Mentioned|p101|||Suggested map symbol||||||
14873|Parilla Sand|30905|6|Mentioned|p146|||||||||
14873|Parilla Sand|30934|6|Mentioned|Map legend|Pliocene|Pliocene|Equivalence with Dorodong Sand||||||
14873|Parilla Sand|30935|6|Mentioned|Map legend|Pliocene|Pliocene|||||||
14873|Parilla Sand|30936|6|Mentioned|Map legend|Miocene|Miocene|||||||
14873|Parilla Sand|30994|6|Mentioned|Fig. 2|||||||||
14873|Parilla Sand|30996|3|Fully described|p31|||Refers Firman (1971).||||||27-OCT-08
14873|Parilla Sand|31554|6|Mentioned|p13|||||||||
14873|Parilla Sand|31624|6|Mentioned|p125|||||||||
14873|Parilla Sand|31743|5|Briefly described|p8|||||||||
14873|Parilla Sand|31744|6|Mentioned|p427|||||||||
14873|Parilla Sand|31745|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
14873|Parilla Sand|31746|3|Fully described|p196|||||||||
14873|Parilla Sand|31747|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
14873|Parilla Sand|31920|4|Described|p59|||See also Fig 3-2||||||
14873|Parilla Sand|31952|6|Mentioned|p7|||||||||
14873|Parilla Sand|32225|6|Mentioned|p22|||||||||
14873|Parilla Sand|32426|5|Briefly described|p141|||||||||
14873|Parilla Sand|32432|5|Briefly described|Table 1|||||||||
14873|Parilla Sand|32439|6|Mentioned|p99|||||||||
14873|Parilla Sand|32859|4|Described|p68|||Upper Pliocene.||||||14-JAN-09
14873|Parilla Sand|32861|5|Briefly described|Table 1|||U.Pliocene||||||
14873|Parilla Sand|33048|6|Mentioned|p197|||||||||
14873|Parilla Sand|33725|6|Mentioned|p9|||Small sinkholes||||||
14873|Parilla Sand|33826|6|Mentioned|p42|||Strat. table||||||
14873|Parilla Sand|33834|5|Briefly described|p11|||||||||
14873|Parilla Sand|34114|4|Described|p50|||Upper Pliocene||||||
14873|Parilla Sand|34180|6|Mentioned|p212|||Late Pliocene. Equivalent Norwest Bend Formation.||||||
14873|Parilla Sand|34191|6|Mentioned|Map legend|late Pliocene|late Pliocene|||||||
14873|Parilla Sand|34308|6|Mentioned|Fig.84|||Yatalan. See P186||||||
14873|Parilla Sand|34313|6|Mentioned|p165|||See also P166. Tertiary||||||
14873|Parilla Sand|34459|4|Described|p11|||U.Pliocene||||||
14873|Parilla Sand|34460|4|Described|p164|||||||||
14873|Parilla Sand|34735|4|Described|p33|||Also mention p31.||||||14-JAN-09
14873|Parilla Sand|34757|6|Mentioned|Fig.3|||||||||
14873|Parilla Sand|34758|6|Mentioned|Fig.2|||||||||
14873|Parilla Sand|34813|6|Mentioned|p63|||||||||
14873|Parilla Sand|35066|6|Mentioned|p216|||||||||
14873|Parilla Sand|35071|6|Mentioned|Table 1|||||||||
14873|Parilla Sand|35091|6|Mentioned|p30|||||||||
14873|Parilla Sand|35097|6|Mentioned|Fig.4|||||||||
14873|Parilla Sand|35131|6|Mentioned|p8|||||||||
14873|Parilla Sand|35172|6|Mentioned|p131|||||||||
14873|Parilla Sand|35174|6|Mentioned|p167|||||||||
14873|Parilla Sand|35187|6|Mentioned|Table1|||||||||
14873|Parilla Sand|35200|6|Mentioned|Map legend|Pliocene|Pliocene|||||||
14873|Parilla Sand|35232|5|Briefly described|Table.3|||||||||
14873|Parilla Sand|35272|6|Mentioned|p281|||||||||
14873|Parilla Sand|35274|6|Mentioned|p425|||||||||
14873|Parilla Sand|35285|5|Briefly described|p414|||||||||
14873|Parilla Sand|35541|6|Mentioned|Fig.2|||Geological section of Tertiary and Quaternary sediments||||||
14873|Parilla Sand|36492|6|Mentioned|Fig.1|||||||||
14873|Parilla Sand|37796|6|Mentioned|p161|||||||||
14873|Parilla Sand|37809|6|Mentioned|p5|||||||||
14873|Parilla Sand|37873|4|Described|p2|||||||||
14873|Parilla Sand|38068|6|Mentioned|Fig.7|||See also Fig.8.||||||
14873|Parilla Sand|38601|6|Mentioned|Fig.2|||||||||
14873|Parilla Sand|39322|6|Mentioned|Fig.3|||||||||
14873|Parilla Sand|39329|6|Mentioned|p483|||||||||
14873|Parilla Sand|39967|4|Described|p44|||||||||
14873|Parilla Sand|40003|5|Briefly described|p39|||See also Table 8.||||||
14873|Parilla Sand|40230|6|Mentioned|Fig.1|||||||||
14873|Parilla Sand|40380|6|Mentioned|p221|||||||||
14873|Parilla Sand|40643|6|Mentioned|p157|||||||||
14873|Parilla Sand|40795|5|Briefly described|p80|||||||||
14873|Parilla Sand|41511|5|Briefly described|p19, p21|||||||||
14873|Parilla Sand|41537|6|Mentioned|p350|||||||||
14873|Parilla Sand|41599|6|Mentioned|p192|||||||||
14873|Parilla Sand|41642|6|Mentioned|p216|||||||||
14873|Parilla Sand|41765|6|Mentioned|p42|||||||||
14873|Parilla Sand|41848|6|Mentioned|p357|||Underlies Coonambidgal Formation, Blanchetown Formation, Age Pliocene (P267, 358)||||||
14873|Parilla Sand|41868|5|Briefly described|p552|||See also P579||||||
14873|Parilla Sand|42115|6|Mentioned|p7|||||||||
14873|Parilla Sand|42125|5|Briefly described|p137|||||||||
14873|Parilla Sand|42126|6|Mentioned|p150|||||||||
14873|Parilla Sand|42129|6|Mentioned|Table 1 P253|||||||||
14873|Parilla Sand|42130|6|Mentioned|Fig.3 P265|||||||||
14873|Parilla Sand|42132|6|Mentioned|Fig.5 P298|||||||||
14873|Parilla Sand|42134|4|Described|p339|||||||||
14873|Parilla Sand|42137|6|Mentioned|p370|||||||||
14873|Parilla Sand|42138|6|Mentioned|p392|||||||||
14873|Parilla Sand|42184|6|Mentioned|Fig.2 P348|||||||||
14873|Parilla Sand|42443|6|Mentioned|p4|||||||||
14873|Parilla Sand|42454|5|Briefly described|p12||Pliocene|||||||
14873|Parilla Sand|42509|4|Described|p2|||||||||
14873|Parilla Sand|42510|5|Briefly described|p35|||||||||
14873|Parilla Sand|42512|5|Briefly described|p68|||||||||
14873|Parilla Sand|42513|6|Mentioned|p96|||||||||
14873|Parilla Sand|42514|5|Briefly described|p116|||||||||
14873|Parilla Sand|42515|5|Briefly described|p134|||||||||
14873|Parilla Sand|42516|6|Mentioned|p152|||||||||
14873|Parilla Sand|42517|5|Briefly described|p169|||||||||
14873|Parilla Sand|42518|5|Briefly described|p185|||||||||
14873|Parilla Sand|42519|5|Briefly described|p205|||||||||
14873|Parilla Sand|42594|5|Briefly described|p247|||Pliocene||||||
14873|Parilla Sand|42635|6|Mentioned|p94|||||||||
14873|Parilla Sand|42717|5|Briefly described|map legend|Pliocene||||||||
14873|Parilla Sand|42720|5|Briefly described|map legend|Pliocene||||||||
14873|Parilla Sand|42813|5|Briefly described|p24|||||||||
14873|Parilla Sand|42827|3|Fully described|p270|||see also Fig 8.4||||||
14873|Parilla Sand|42881|4|Described|Fig.3, P84|||||||||
14873|Parilla Sand|42966|1|Redefined|Table 26, p162|Late Pliocene||||||||
14873|Parilla Sand|43053|5|Briefly described|Map Legend|Pliocene|Pliocene|Fluviolacustrine and coastal, siliceous and clayey sand.||||||25-MAY-05
14873|Parilla Sand|43073|4|Described|p12,Table 3|||||||||
14873|Parilla Sand|43195|5|Briefly described|Map Legend||Late Pleistocene|see also commentary on back of map.||||||
14873|Parilla Sand|43218|4|Described|Fig.3,p22||Tertiary|||||||
14873|Parilla Sand|43258|5|Briefly described|Map Legend||Pliocene|||||||
14873|Parilla Sand|43261|5|Briefly described|Map Legend|Miocene|Oligocene|||||||
14873|Parilla Sand|43298|6|Mentioned|Map Legend||Pliocene|||||||
14873|Parilla Sand|43493|6|Mentioned|32||Pliocene|||||||
14873|Parilla Sand|43578|6|Mentioned|p342|||||||||
14873|Parilla Sand|43627|6|Mentioned|p6||Pliocene|||||||
14873|Parilla Sand|43655|5|Briefly described|p40-846|||||||||
14873|Parilla Sand|43669|4|Described|p22-23|||||||||
14873|Parilla Sand|43846|5|Briefly described|14||Miocene|||||||
14873|Parilla Sand|44133|5|Briefly described|p161|Late Pliocene|Late Pliocene|Geological Province: Murray Basin. Overlies Loxton Sand.||||||
14873|Parilla Sand|44186|5|Briefly described|Map Legend|Pliocene|Miocene|||||||
14873|Parilla Sand|44188|5|Briefly described|Map Legend|Pleistocene|Pliocene|Geological province: Murray Basin. Poorly consolidated to consolidated, poorly sorted, mediuym- to coarse-grained quartz and sandstone.||||||15-MAY-08
14873|Parilla Sand|44931|5|Briefly described|Map Legend|Tertiary|Tertiary|Littoral sand deposits.||||||14-JUN-06
14873|Parilla Sand|46839|6|Mentioned|p82|||||||||
14873|Parilla Sand|46909|6|Mentioned|p83|||See also Fig.1||||||
14873|Parilla Sand|49038|5|Briefly described|p26|||See also P40||||||
14873|Parilla Sand|49040|6|Mentioned|p12|||||||||
14873|Parilla Sand|50154|1|Redefined|p42, p133, p136-137|Early Pliocene|Late Miocene|Overlies the Renmark Group, Murray Group, Bookpurnong beds and the Grampians Group. Overlain by Lowan Sand. Synonymous with the Diapur Sandstone. Geological Province: Murray Basin. Thickness: 40-150m. In part correlative with the Bookpurnong beds.||||||10-NOV-10
14873|Parilla Sand|50155|5|Briefly described|Map Legend|Pliocene|Miocene|Sand, silt, commonly forms strand lines||||||
14873|Parilla Sand|50156|5|Briefly described|Map Legend|Pliocene|Miocene|Marine: sand, silt; commonly forms strand lines||||||
14873|Parilla Sand|50157|5|Briefly described|Map Legend|Pliocene|Miocene|Overlies Duddo Limestone. Overlain by Lowan Sand. Marine: sand, silt; commonly forms strand lines||||||25-JUN-04
14873|Parilla Sand|50158|5|Briefly described|Map Legend|Pliocene|Miocene|Marine: sand, silt; commonly forms strand lines||||||25-JUN-04
14873|Parilla Sand|50159|5|Briefly described|Map Legend|Pliocene|Miocene|Marine: sand, silt; commonly forms strand lines||||||
14873|Parilla Sand|50160|5|Briefly described|Map Legend|Pliocene|Miocene|||||||
14873|Parilla Sand|50161|5|Briefly described|Map Legend|Pliocene|Miocene|Marine: sand, silt; commonly forms strand lines||||||
14873|Parilla Sand|50162|5|Briefly described|Map Legend|Pliocene|Miocene|Overlies Duddo Limestone, Marn Mering Granodiorite, Schofield Granite, Kout Norien Granodiorite, Tuloona Granodiorite and Glenelg Metamorphic Complex. Marine: sand, silt; commonly forms strand lines||||||25-JUN-04
14873|Parilla Sand|50163|5|Briefly described|Map Legend|Pliocene|Miocene|Overlain by Lowan Sand. Overlies Duddo Formation. Marine: sand, silt; commonly forms strand lines||||||25-JUN-04
14873|Parilla Sand|50164|5|Briefly described|Map Legend|Pliocene|Miocene|Sand, silt, commonly forms strand lines.||||||
14873|Parilla Sand|60451|5|Briefly described|p30, 95 Fig. 61, 99|Early Pliocene|Late Miocene|Type section in text. Maximum Thickness: 25m+. Overlies: White Hills Gravel, conformably overlies Calivil Formation.||||||
14873|Parilla Sand|60452|4|Described|p37|Early Pliocene|Late Miocene|First named Loxton Sand; upper part then named Parilla Sand (also Diapur Sand). Also termed Loxton-Parilla Sand (Vic-SA). Divided into Kerang Sand, Tragowel and Wandella Sand Members by Macumber (1983). Disconformably overlain by Shepparton Formation.||||||
14873|Parilla Sand|60454|5|Briefly described|Map Legend|Neogene|Neogene|Unit does not appear on this map.||||||
14873|Parilla Sand|60456|5|Briefly described|Map Legend|Neogene|Neogene|Unit does not appear on this map.||||||
14873|Parilla Sand|60457|5|Briefly described|Map Legend|Neogene|Neogene|Littoral deposits; well sorted, fine to medium grained quartz sandstone; well bedded; abundant lag horizons containing shelly fossils, pebble beds, rounded ironstone fragments.||||||
14873|Parilla Sand|60458|5|Briefly described|Map Legend|Neogene|Neogene|Littoral deposits: well sorted, fine to medium grained quartz sandstone; well bedded; abundant lag horizons.||||||
14873|Parilla Sand|60461|5|Briefly described|Map legend|Pliocene|Miocene|Littoral to near shore marine deposits. Clay, silt, fine to coarse-grained quartz sand, minor quartz gravel, minor heavy mineral sands with disseminated zircon, tourmaline, ilmenite & rutile; commonly ferruginised; sorting good to moderate, cross-bedded.||||||06-OCT-04
14873|Parilla Sand|60462|5|Briefly described|Map Legend|Neogene|Neogene|Marginal marine sand, lesser silt and gravel; swales rarely weakly magnetic (to 2 nT); thorium high where outcropping.||||||15-SEP-04
14873|Parilla Sand|60491|4|Described|p16, p21-22|Pliocene|Late Miocene|Interfingers with the Calivil Formation. Disconformably overlies the Renmark Group sediments. Disconformably overlain by the Shepparton Formation. Max. thickness: 100m. Geological Province: Murray Basin.||||||
14873|Parilla Sand|60492|5|Briefly described|Map Legend|Pliocene|Miocene|Overlies the Renmark Group. Overlain by the Shepparton Formation. Paralic to marginal marine: moderately sorted sandstone and unconsolidated sand; ferruginised in part; fossiliferous; dunes highlighted.||||||
14873|Parilla Sand|60493|5|Briefly described|Map Legend|Neogene|Paleogene|Marginal marine strand deposits: linear N-S magnetic features up to about 5 nT; interdunes have slightly higher K, Th, U responses.||||||07-NOV-08
14873|Parilla Sand|60540|5|Briefly described|p999,p1000 Fig.2, p1002|Pliocene|Pliocene|||||Lateral equivalent to Moorna Formation and upper Norwest Bend Formation.|Aeolian and terrestrial sediments.|06-FEB-18
14873|Parilla Sand|60543|5|Briefly described|Map legend|Tertiary|Tertiary|||||||23-DEC-09
14873|Parilla Sand|60591|5|Briefly described|Map Legend|Pliocene|Miocene|Overlies the Renmark Group and Calivil Formation. Quartz pebbles, quartz sandstone, minor clay and silt; poor- to moderate-sorting and rounding, open framework, weakly cemented; minor burrows.||||||20-JAN-05
14873|Parilla Sand|60592|5|Briefly described|Map Legend|Pliocene|Miocene|Overlies the Renmark Group and Calivil Formation. Quartz pebbles, quartz sandstone, minor clay and silt; poor- to moderate-sorting and rounding, open framework, weakly cemented; minor burrows.||||||20-JAN-05
14873|Parilla Sand|60593|5|Briefly described|Map Legend|Pliocene|Miocene|Overlies the Renmark Group and Calivil Formation. Quartz pebbles, quartz sandstone, minor clay and silt; poor- to moderate-sorting and rounding, open framework, weakly cemented; minor burrows.||||||20-JAN-05
14873|Parilla Sand|60595|5|Briefly described|Map Legend|Pliocene|Miocene|Overlies the Renmark Group and Calivil Formation. Quartz pebbles, quartz sandstone, minor clay and silt; poor- to moderate-sorting and rounding, open framework, weakly cemented; minor burrows.||||||20-JAN-05
14873|Parilla Sand|60596|5|Briefly described|Map Legend|Pliocene|Miocene|Overlies the Renmark Group and Calivil Formation. Quartz pebbles, quartz sandstone, minor clay and silt; poor- to moderate-sorting and rounding, open framework, weakly cemented; minor burrows.||||||20-JAN-05
14873|Parilla Sand|60597|5|Briefly described|Map Legend|Pliocene|Miocene|Paralic to fluvial deposits: nonmagnetic.||||||
14873|Parilla Sand|60599|5|Briefly described|p7, p15, p80||Early Pliocene|Shallow marine and littoral deposits that interfinger with Calivil Formation; unconformably overlies Wild Duck Formation. Geological Province: Murray Basin.||||||
14873|Parilla Sand|60953|5|Briefly described|Map Legend|Pliocene|Pliocene|Fluviolacustrine and coastal aeolian, siliceous and clayey sand.||||||
14873|Parilla Sand|61108|5|Briefly described|map legend|Pliocene|Pliocene|Fluviolacustrine and coastal aeolian, siliceous and clayey sand.||||||
14873|Parilla Sand|61155|5|Briefly described|p5, p6|Pliocene|Pliocene|Fluvial clastic deposits. Geological Province:Murray Basin.||||||
14873|Parilla Sand|61180|5|Briefly described|p7|Pliocene|Late Miocene|Consists of well-sorted silt and fine-to coarse-grained quartz sand, with rare gravel.||||||
14873|Parilla Sand|61181|6|Mentioned|p28, p137|Pliocene|Miocene|See also Parilla Sands. See also p153 Fig. 47.||||||
14873|Parilla Sand|61183|4|Described|p18 Fig. 9, p67|Tertiary|Tertiary|Widespread quartz and carbonate sand. Includes subsurface occurrences of fossiliferous marine sandstone. See also p19, p129.||||||
14873|Parilla Sand|61185|5|Briefly described|p58, p15, p63|Pliocene|Late Miocene|Interfingers with and conformably underlies Calivil Formation. Geological Province: Murray Basin. Shallow marine and littoral. Interpreted as lateral equivalent of Yando Clay.||||||07-FEB-11
14873|Parilla Sand|61314|5|Briefly described|p129|Late Pliocene|Late Pliocene|Includes the Loxton Sand. Geological Province: Murray Basin.||||||
14873|Parilla Sand|61964|6|Mentioned|p139|||Regional correlative is Calivil Sand (Renmark Group). Geological Province: Murray Basin.||||||
14873|Parilla Sand|63124|6|Mentioned|p94||Pliocene|Geological Province: Gambier Basin.||||||
14873|Parilla Sand|63446|5|Briefly described|Map legend|Pliocene|Miocene||||||Marine: sand, silt.|
14873|Parilla Sand|64096|5|Briefly described|p283||Early Pliocene|Unconformably overlies Lake Boga Granite as a 1-5 m-thick layer of sandy sediment.||||||
14873|Parilla Sand|64237|5|Briefly described|p17, p18 Fig. 2, p19 Fig. 2b|Late Pliocene|Pliocene|Part of original stratigraphic scheme (Ludbrook 1961) tog. with Norwest Bend Fm and Loxton Sand.............Original configuration for this trio - Norwest Bend Fm/Parilla Sand/Loxton Sand was retained in the stratigraphic revision by Rogers et al (1998).||||||29-JUL-08
14873|Parilla Sand|65194|6|Mentioned|p25-27|||Forms an aquifer at Lake Tyrrell.||||||
14873|Parilla Sand|65552|5|Briefly described|p5 Fig. 3|Late Pliocene|Late Pliocene|Only differentiated in western Murray Basin. Elsewhere part of 'Loxton-Parilla Sands'. Where differentiated overlies Loxton Sands, underlies Blanchetown Clay.||||||
14873|Parilla Sand|65715|5|Briefly described|p15 Tb.8|||Possibly junior synonym of Loxton Sand in Victoria [probably still current in SA].||||||
14873|Parilla Sand|65719|5|Briefly described|p7|Miocene|Miocene|In Murray Basin. Lateral equivalent of Mystic Park Formation. Marginal marine or paralic. Late Miocene.||||||10-MAY-12
14873|Parilla Sand|65969|5|Briefly described|p3, p27 Tb.3.3, p30-1|Pliocene|Pliocene|Murray Basin. Equivalent to Shepparton Formation. Marginal marine to paralic sand. Relics of sand sheets on the sides of valleys. No magnetic response; high Th radiometric response where subsequently lateritised, elsewhere low in all channels.||||||
14873|Parilla Sand|66002|5|Briefly described|p13 Tb.9, p18-19|||Of Firman 1965. Aeolian. Difficult to distinguish from underlying marine Loxton Sand. Forms ridges and swales with an east-west pattern||||||
14873|Parilla Sand|66286|6|Mentioned|p181.|Pliocene|Miocene|Deposited during regression of a marine incursion into western Murray Basin. Its aeolian and associated sediments are correlated with the oyster-rich, upper of two informal members of the Norwest Bend Formation.||||||
14873|Parilla Sand|66287|6|Mentioned|p26, 33|Neogene|Neogene|Of Firman 1966 and 1973. Previous name for (minor) non-marine part of the Loxton-Parilla Sands.||||||20-APR-12
14873|Parilla Sand|67127|6|Mentioned|p73|||||||Overlies the Geera Clay.||
14873|Parilla Sand|67347|6|Mentioned|p836, 843|Early Pliocene|Early Pliocene|Generally saline aquifer.||||Underlain by the Lake Boga Granite.||11-MAY-12
14873|Parilla Sand|67462|5|Briefly described|Map legend.|Pliocene|Pliocene|Murray Basin.||||||
14873|Parilla Sand|68189|5|Briefly described|p4, p6 Fig.1, p19 Fig.8, pp25-32|Miocene|Miocene|Littoral to near-shore marine sequence which regresses to the west. Dominant near-surface unit where the Murray Basin is present in ST ARNAUD.|< 6 Ma|||Disconformably underlain by the Olney Formation. Conformably overlain and interfingered by the Shepparton Formation. Overlain by the Geera Clay. Underlain by the Winnambool Formation.|Comprises sand (often cross bedded).|
14873|Parilla Sand|68194|5|Briefly described|p6, p9, p11, p17, p20-21, p23-31, p34-36|Pliocene|Pliocene|See also p40, p43 Fig.42, p44, p55-57, p73-74. Blackburn (1962). Strandlines form ridged marine plains. Also appears as Parilla Sand Formation on p9 and p11. Called Loxton Sand in SA. Regolith and remote sensing profiles described.||Unit in Wunghnu Group.||Disconformably overlies Geera Clay. Is overlain disconformably by Shepparton Formation. Lateral facies equivalent of Bookpurnong beds.|Variably-sorted, fine- to very coarse-grained, subangular to subrounded quartz sandstone.|
14873|Parilla Sand|68548|5|Briefly described|p13|Pliocene|Pliocene|Late Pliocene age.||||Laterally equivalent to the Norwest Bend Formation and the Moorna Formation.|Comprises aeolian and associated terrestrial sediments.|
14873|Parilla Sand|68715|5|Briefly described|p31 Fig.5|Pliocene|Miocene|Murray Basin. Late Miocene maximum age.||Of the Murray Group.||||
14873|Parilla Sand|70718|5|Briefly described|p23|||Parilla Sands used p104.||||Equivalent to Shepparton Fomation?||30-MAY-19
14873|Parilla Sand|70961|14|Not recorded|p138|||Refers to Firman (1966).||||||
14873|Parilla Sand|72445|6|Mentioned|App.7 p7 Fig.4.|Pliocene|Pliocene|Shown on the 'Lithostratigraphy of Cenozoic sediments in the Murray Basin' (from Brown & Stephenson 1991).||||Shown as overlying Loxton Sands and equivalent to Norwest Bend Formation and underlying Blanchetown Clay.|Shown as including sand.|
14873|Parilla Sand|73188|5|Briefly described|p314, p320|Pliocene|Pliocene|Murray Basin.|||||Shallow marine calcareous sand, fluvial and coastal barrier sands.|
14873|Parilla Sand|73228|4|Described|p51, p58|||Derived mainly from Loxton Sand by aeolian and fluvial reworking and may include large transgressive dune complexes, as well as lacustrine and fluvial deposits laid down in depressions between stranded coastal ridges.||||Underlain by Loxton Sand.|Unfossiliferous, nonmarine, fine- to medium-grained clayey quartz sand with thin beds of sandy clay.|
14873|Parilla Sand|73496|5|Briefly described|Map legend|Pliocene|Miocene|||Wunghnu Group|||Magnetic interdunes several km long parallel arcuate magnetic high (about 10 nT) trending north to corthwest and concave west; where not covered or eroded, interdune topographic lows are radiometric highs.|
14873|Parilla Sand|73497|5|Briefly described|Map legend|Pliocene|Miocene|||Wunghnu Group|||Gravel, sand and silt: no distinctive magnetic responses, low K, Th and variable U.|
14873|Parilla Sand|73505|4|Described|p1-2, p4, p11-14, p23, p36, p38|Pliocene|Late Miocene|Murray Basin. Host to heavy mineral sands. Topography of upper surface is broad convex-west arcuate ridges, eroded away in places. Minor magnetic highs correlate with topographic lows. Th high where lateratised or mineralised.||Wunghnu Group||Overlies Bookpurnong beds, Calivil Formation, 'Middle Renmark Group', underlies Blanchetown Clay, sequence/time equivalent of Shepparton Formation and Bookpurnong beds|Marginal marine sand dunes.|
14936|Patchawarra Formation|13497|4|Described|iv, v, vi, viii, ix, x|Artinskian|Asselian|Cooper Basin.  Named for the Patchawarra Bore by Kapel (1972). Petrography and lithology described in detail. A sedimentary facies log is provided. The lower part of this formation is lithologically similar to the Tirrawarra Sandstone.  Up to 680m thick in the Nappamerri Trough. Coal and carbonaceous shale of this unit are the primary source rocks of the Cooper Basin. Total thickness up to 373.4m. Hosts large gas reservoirs and is sealed by Murteree Shale. Informally referred to a as  "lower" and "upper" subunits. See also  xi, xii, p55, p61, p63-p64, p69 fig 6.1, p70-p73, p75, p86-p94, p99, p119, p122, p124-p127, p129, p131, p132 tbl 8.1, p138 fig 8.17, p139 fig 8.18, p141, p144 fig 9.2, p146, p148-p154, p157, p159-p161, p168-p172, p174-p176, p182-p184, p190-p196, p204-p205, p208, p216.||Gidgealpa Group|Includes the Malabine Coal.|Overlies and interfingers with the Tirrawarra Sandstone. Overlies the Merrimelia Formation. Conformably overlain by the Murteree Shale. Disconformably overlain by the Toolachee Formation.|Interbedded fine to medium-grained, locally coarse-grained and pebbly sandstone, grey to black siltstone, shale and coal.|
14936|Patchawarra Formation|13516|6|Mentioned|p147 fig 5, p148|Early Permian|Early Permian|From Cooper Basin. Loosely correlated with top of the Reids Dome beds and basal Cattle Creek Formation.||||||
14936|Patchawarra Formation|22527|5|Briefly described|p 1, 2, 3, Fig1, 3|||||||||
14936|Patchawarra Formation|22839|6|Mentioned|P33|||||||||
14936|Patchawarra Formation|22883|6|Mentioned|P29|||||||||
14936|Patchawarra Formation|22924|6|Mentioned|49|||||||||
14936|Patchawarra Formation|23154|5|Briefly described|Map Legend|Early Permian|Early Permian|Geological Province: Cooper Basin.  Of the Gidgealpa Group.||||||22-NOV-06
14936|Patchawarra Formation|23155|4|Described|p17|Early Permian|Early Permian|Unit up to 450m thick.  Spore pollen assemblages are Asselian - Kungurian in age.||||||
14936|Patchawarra Formation|23356|5|Briefly described|26 Tab.2|Early Permian|Early Permian|||||||
14936|Patchawarra Formation|23359|5|Briefly described|73|Early Permian|Early Permian|||||||
14936|Patchawarra Formation|23375|4|Described|Fig2 p265,285|Artinskian|Sakmarian|In the Cooper Basin.||||||22-NOV-06
14936|Patchawarra Formation|23832|4|Described|p328|Permian|Permian|Of Gidgealpa Group. Geological Province: Cooper Basin.||||||
14936|Patchawarra Formation|24199|5|Briefly described|p512|Early Permian|Early Permian|Geological Province: Cooper Basin.||||||
14936|Patchawarra Formation|24204|5|Briefly described|p284|Permian|Permian|Geological Province: Cooper Basin.||||||
14936|Patchawarra Formation|24210|5|Briefly described|p133 Fig. 2|Permian|Permian|Of the Gidgealpa Group.  Overlies the Tirrawarra and Merrimelia Formations.  Geological Province: Cooper Basin.  See also p132.||||||22-NOV-06
14936|Patchawarra Formation|24212|4|Described|p65,  p67 Fig. 3p|Early Permian|Early Permian|Age: 280Ma.  Geological Province: Cooper Basin.||||||
14936|Patchawarra Formation|24372|6|Mentioned|p22|||Geological Province: Cooper Basin.||||||
14936|Patchawarra Formation|24620|6|Mentioned|p6|||Referred to in text as Patchawarra only - intended to be Patchawarra Formation.  Geological Province: Cooper Basin.||||||
14936|Patchawarra Formation|29387|6|Mentioned|Table 2|||Refs to Gatehouse(1972).||||||
14936|Patchawarra Formation|29389|6|Mentioned|p18|||Permian.||||||
14936|Patchawarra Formation|29391|6|Mentioned|Table 5|||See p23.||||||22-NOV-06
14936|Patchawarra Formation|29513|6|Mentioned|p23|||||||||
14936|Patchawarra Formation|29515|6|Mentioned|p14|||||||||
14936|Patchawarra Formation|29518|6|Mentioned|p24|||||||||
14936|Patchawarra Formation|29721|6|Mentioned|p182|||||||||
14936|Patchawarra Formation|29729|6|Mentioned|p266|||||||||
14936|Patchawarra Formation|30519|5|Briefly described|p73|||See also p75. Part of Gidgealpa Group.||||||22-NOV-06
14936|Patchawarra Formation|30540|6|Mentioned|p65|||General Geology||||||
14936|Patchawarra Formation|30542|6|Mentioned|p50|||||||||
14936|Patchawarra Formation|30544|6|Mentioned|p52|||||||||
14936|Patchawarra Formation|30825|6|Mentioned|p37|||||||||
14936|Patchawarra Formation|30873|3|Fully described|p14|||||||||
14936|Patchawarra Formation|30921|6|Mentioned|Map legend|Artinskian|Sakmarian|Age is Sakamarian - Artinskian.||||||22-NOV-06
14936|Patchawarra Formation|31591|3|Fully described|p54|||See also p55, 56, 57. Early to Lower Permian.||||||05-OCT-06
14936|Patchawarra Formation|32696|6|Mentioned|Fig.4|||See also Figs. 6,7,8,9||||||
14936|Patchawarra Formation|33074|6|Mentioned|p260|||||||||
14936|Patchawarra Formation|33331|6|Mentioned|p38|||||||||
14936|Patchawarra Formation|33489|6|Mentioned|Fig.2|||Refers Kapel (1972) and Gatehouse (1972)||||||22-NOV-06
14936|Patchawarra Formation|33523|6|Mentioned|p26|||||||||
14936|Patchawarra Formation|33971|6|Mentioned|p33|||||||||
14936|Patchawarra Formation|33976|6|Mentioned|p9|||Similar to Purni Formation.||||||22-NOV-06
14936|Patchawarra Formation|34839|6|Mentioned|Fig.2|||||||||
14936|Patchawarra Formation|35067|6|Mentioned|Fig.4|||||||||
14936|Patchawarra Formation|35068|6|Mentioned|Fig.3|||Discussed p54.||||||22-NOV-06
14936|Patchawarra Formation|35151|6|Mentioned|p147|||||||||
14936|Patchawarra Formation|35279|6|Mentioned|p19|||||||||
14936|Patchawarra Formation|35457|6|Mentioned|p627|||Also Fig.4 biostratigraphic relationships||||||
14936|Patchawarra Formation|35573|6|Mentioned|Fig.7|||Generalised stratigraphy - Southern Cooper Basin||||||
14936|Patchawarra Formation|35845|4|Described|p24|||Lithology and depositional environments. See also Fig.25||||||05-OCT-06
14936|Patchawarra Formation|36099|6|Mentioned|p191|||||||||
14936|Patchawarra Formation|36172|6|Mentioned|Appendix|||||||||
14936|Patchawarra Formation|36613|6|Mentioned|p1864|||||||||
14936|Patchawarra Formation|36910|6|Mentioned|p60|||||||||
14936|Patchawarra Formation|36917|6|Mentioned|Fig.1|||||||||
14936|Patchawarra Formation|36924|6|Mentioned|Table 1|||||||||
14936|Patchawarra Formation|37065|6|Mentioned|p30|||||||||
14936|Patchawarra Formation|37103|5|Briefly described|p266|||||||||
14936|Patchawarra Formation|37287|6|Mentioned|p36|||||||||
14936|Patchawarra Formation|37703|6|Mentioned|p2240|||||||||
14936|Patchawarra Formation|37855|6|Mentioned|Fig.2|||||||||
14936|Patchawarra Formation|37917|6|Mentioned|Fig.2|||||||||
14936|Patchawarra Formation|38958|5|Briefly described|p491|||||||||
14936|Patchawarra Formation|38977|6|Mentioned|Fig.1|||||||||
14936|Patchawarra Formation|39252|5|Briefly described|p20|||See also p13 and p22.||||||22-NOV-06
14936|Patchawarra Formation|39254|5|Briefly described|p46|||See also p47.||||||22-NOV-06
14936|Patchawarra Formation|39255|6|Mentioned|p51|||||||||
14936|Patchawarra Formation|39261|6|Mentioned|Fig. 9|||||||||
14936|Patchawarra Formation|39264|6|Mentioned|Fig. 13|||||||||
14936|Patchawarra Formation|39265|6|Mentioned|Fig. 3|||||||||
14936|Patchawarra Formation|39276|6|Mentioned|Fig. 2|||||||||
14936|Patchawarra Formation|39445|5|Briefly described|Table 8|||See also p94.||||||22-NOV-06
14936|Patchawarra Formation|39478|6|Mentioned|Table 1|||||||||
14936|Patchawarra Formation|39494|6|Mentioned|Fig.3|||||||||
14936|Patchawarra Formation|39757|6|Mentioned|p1601|||||||||
14936|Patchawarra Formation|40030|6|Mentioned|p131|||See also Fig.3||||||
14936|Patchawarra Formation|40249|6|Mentioned|p45|||||||||
14936|Patchawarra Formation|40544|6|Mentioned|p157|||||||||
14936|Patchawarra Formation|40637|6|Mentioned|Fig.2|||||||||
14936|Patchawarra Formation|41060|6|Mentioned|Fig.5|||||||||
14936|Patchawarra Formation|41099|6|Mentioned|p185|||||||||
14936|Patchawarra Formation|41123|6|Mentioned|p180|||||||||
14936|Patchawarra Formation|41131|5|Briefly described|Table 1|||||||||
14936|Patchawarra Formation|41164|6|Mentioned|p422|||||||||
14936|Patchawarra Formation|41165|6|Mentioned|Fig.18|||||||||
14936|Patchawarra Formation|41166|6|Mentioned|p379|||||||||
14936|Patchawarra Formation|41183|6|Mentioned|Fig.3 p308|||||||||
14936|Patchawarra Formation|41184|6|Mentioned|p346|||||||||
14936|Patchawarra Formation|41189|6|Mentioned|p249|||||||||
14936|Patchawarra Formation|41198|6|Mentioned|p44|||||||||
14936|Patchawarra Formation|41214|6|Mentioned|p256|||||||||
14936|Patchawarra Formation|41221|6|Mentioned|p392|||||||||
14936|Patchawarra Formation|41226|6|Mentioned|p22|||||||||
14936|Patchawarra Formation|41247|6|Mentioned|p117|||||||||
14936|Patchawarra Formation|41267|6|Mentioned|p256|||||||||
14936|Patchawarra Formation|41288|6|Mentioned|p156|||||||||
14936|Patchawarra Formation|41491|6|Mentioned|p180|||||||||
14936|Patchawarra Formation|41595|5|Briefly described|p30|||||||||
14936|Patchawarra Formation|41689|6|Mentioned|Table 1|||||||||
14936|Patchawarra Formation|41707|6|Mentioned|Fig.8|||||||||
14936|Patchawarra Formation|41712|6|Mentioned|p282|||||||||
14936|Patchawarra Formation|41720|6|Mentioned|p370|||||||||
14936|Patchawarra Formation|42064|6|Mentioned|Fig.5 P.171|||||||||
14936|Patchawarra Formation|42085|6|Mentioned|Fig.2 P374|||||||||
14936|Patchawarra Formation|42150|6|Mentioned|p65|||||||||
14936|Patchawarra Formation|42153|6|Mentioned|p361|||||||||
14936|Patchawarra Formation|42154|6|Mentioned|p361|||||||||
14936|Patchawarra Formation|42187|6|Mentioned|Fig.3 P318|||||||||
14936|Patchawarra Formation|42256|6|Mentioned|Fig.1 P243|||||||||
14936|Patchawarra Formation|42395|6|Mentioned|p80|||||||||
14936|Patchawarra Formation|42496|5|Briefly described|App.1 P152, Fig.3 P2|||||||||
14936|Patchawarra Formation|42547|5|Briefly described|p81|||||||||
14936|Patchawarra Formation|42599|6|Mentioned|p624|||In the Cooper Basin.||||||22-NOV-06
14936|Patchawarra Formation|42648|5|Briefly described|p41, p48|||||||||
14936|Patchawarra Formation|42746|5|Briefly described|p6|||In the Cooper Basin.||||||22-NOV-06
14936|Patchawarra Formation|42999|5|Briefly described|Table 2,p90||Early Permian|||||||
14936|Patchawarra Formation|43018|5|Briefly described|Table 1,p386|||||||||
14936|Patchawarra Formation|43105|5|Briefly described|p14|||||||||
14936|Patchawarra Formation|43570|4|Described|p533,Fig.2,p535,|Sakmarian|Asselian|p541-4, p550-552.||||||05-OCT-06
14936|Patchawarra Formation|43628|6|Mentioned|Fig.3||Early Permian|||||||
14936|Patchawarra Formation|43711|6|Mentioned|p19|||||||||
14936|Patchawarra Formation|44133|4|Described|p65 Fig. 8.4, 84|Permain|Permain|Of the Gidgealpa Group. Geological Province: Cooper Basin. Conformably overlies Tirrawarra Sandstone. Maximum Thickness: 680m. Conformably underlies the Murteree Shale.||||||22-NOV-06
14936|Patchawarra Formation|46849|6|Mentioned|Fig. 7|||||||||
14936|Patchawarra Formation|48995|6|Mentioned|Fig.3|||||||||
14936|Patchawarra Formation|60386|6|Mentioned|p296|Artinskian|Sakmarian|Cooper Basin. Non-marine, coal.||||||
14936|Patchawarra Formation|60717|5|Briefly described|p40, p41|Artinskian|Asselian|Of the Gidgealpa Group. Overlain by Murteree Shale; overlies Tirrawarra Sandstone. Thickness: 680m. Geological Province: Cooper Basin. See also Figure 2.||||||31-JAN-08
14936|Patchawarra Formation|61015|6|Mentioned|p46|||||||||
14936|Patchawarra Formation|61250|6|Mentioned|p45|||Contains petroleum systems. Geological Province: Cooper Basin.||||||18-AUG-05
14936|Patchawarra Formation|61614|5|Briefly described|p289, p290, p292, p295, p290 Fig. 2|Early Permian|Early Permian|Of Gidgealpa Group. Geological Province: Cooper Basin. Contain coal and shale lithologies.||||||17-MAR-09
14936|Patchawarra Formation|61616|6|Mentioned|p329, p330, p331, p338, p330 Fig. 2|Early Permian|Early Permian|Of Gidgealpa Group. Geological Province: Cooper Basin.||||||
14936|Patchawarra Formation|61617|6|Mentioned|p343, p344, p346, p346 Tb. 3|Permian|Permian|Net coal thickness: 40-60m. Geological Province: Cooper Basin.||||||
14936|Patchawarra Formation|62537|6|Mentioned|p191 Fig.2. |Early Permian|Early Permian|Cooper Basin.||Unit in Gidgealpa Group.||Overlies Tirrawarra Sandstone. Is overlain by Murteree Shale.||
14936|Patchawarra Formation|62730|5|Briefly described|p352 Fig. 1|Late permian|Early Permian|Geological Province: Cooper Basin.||||||21-APR-08
14936|Patchawarra Formation|62759|5|Briefly described|p1|||Geological Province: Cooper Basin.||||||05-FEB-08
14936|Patchawarra Formation|63978|2|Defined|p11, Fig. 3|Early Permian|Early Permian|Of Gidgealpa Gp.Conformable on Tirrawarra Sst.or unconformable on Merrimelia Fm; conformable below Murteree Shale. In northern Cooper Basin - overlain by Toolachee Formation. Upwardly fining sst.,siltstone, mudstone and coal...detailed lith. included||||||09-APR-13
14936|Patchawarra Formation|64048|5|Briefly described|p63, p64 Tb. 2, p65-66|Permian|Permian|Unconformably overlain by Toolachee Formation where the Murteree and Epsilon Formations, and Roseneath Shale are absent. Source of hydrocarbons - coal measures. Geological Province: Cooper Basin.||||||07-FEB-11
14936|Patchawarra Formation|64197|6|Mentioned|p625 Fig.1c, p630 Fig.7|Middle Permian|Middle Permian|Cooper Basin.||||Underlies the Murteree Shale and Roseneath Shale. Overlies the Tirrawarra Sandstone and Merrimelia Formation.||11-DEC-15
14936|Patchawarra Formation|64232|5|Briefly described|p12|||Geological Province: Cooper Basin/ Weena Trough. Shallow occurrences of thick sub-bituminous coal seams are present in this unit.||||||24-JUL-08
14936|Patchawarra Formation|64665|5|Briefly described|p53 Fig.2, p56.|Early Permian|Early Permian|Cooper Basin. Hosts coal: equivalent to Aramac Coal Measures (Galilee Basin) and Reids Dome beds and Collinsville Coal Measures (Bowen Basin). Contains hydrocarbon source rocks and reservoirs; also thought to have charged the underlying Merrimelia Formation and Tirrawarra Sandstone reservoirs.||||Overlies Tirrawarra Sandstone. Is overlain by Murteree Shale.||
14936|Patchawarra Formation|65489|5|Briefly described|p11, p15-16, p45-49, p55, p73, p91, p96|Artinskian|Asselian|See also p132, p143, p158. Cooper Basin. Major source unit. Gas flow was announced from this unit by Bridge Oil in 1970. Gas and oil reservoir accounting for 32% and 5% respectively of the Basin's production.||Unit in Gidgealpa Group.||Overlies Tirrawarra Sandstone and Merrimelia Formation. Is overlain by Murteree Shale. Is correlated with Purni Formation (Pedirka Basin).|Includes abundant coals and multi-zone high-sinuosity fluvial sandstones.|
14936|Patchawarra Formation|65925|5|Briefly described|Appendix 2.||||||||Siltstone, coal-swamp; sandstone; minor coal. Fluviolacustrine floodplain, minor deltaic environments.|
14936|Patchawarra Formation|67402|5|Briefly described|p90 fig CPR4, p91 tbl CPR1|||Cooper Basin. Prospective reservoir for the storage of carbon dioxide with a potential storage capacity of 3.4 Megatonnes. Deposited in low to moderate energy fluvial environments dominated by highly meandering rivers and their floodplains. Up to 400m thick. See also p90-p94, p98, p99 fig CPR14, p100, p101, p101 tbl CPR2, p104, p105, p268.||Gidgealpa Group||Overlain by the Murteree Shale and Toolachee Formation. Overlies the Tirrawarra Sandstone.|Fining upwards deposits of fine to medium-grained sandstone, siltstone, shale and major coal beds.|
14936|Patchawarra Formation|68068|5|Briefly described|Map legend|Early Permian|Early Permian|Cooper Basin (subsurface only). Stacked channel and upward-fining deposits. Fluvial (point bars, meandering river), backswamp and floodbasin environments. Spore-pollen assemblage is of cold to cool-temperate flora.||Unit in Gidgealpa Group.||Conformably overlies Tirrawarra Formation. Is conformably overlain by Murteree Shale.|Interbedded, grey, buff or brown sandstone (locally pebbly), mudstone with carbonaceous partings and coal; thick coal seams in lower part; upper levels dominated by mudstone with thin interbeds of siltstone and sandstone.|
14936|Patchawarra Formation|68731|5|Briefly described|p200 Fig 3.110, p204, p206, p207|Cisuralian|Cisuralian|Kapel (1972); Gatehouse (1972). ~ 50 to > 500 m thick. Palynofloras are Cisuralian (Gray and McKellar 2002). Authigenic quartz, kaolinite and dicktite are common in sandstones. Coal seams are up to 16m thick. Interdigitates with the Murteree Shale.||Of the Gidgealpa Group.||Underlain/unconformably underlain by the Tirrawarra Sandstone and the Merrimelia Formation respectively. Conformably overlain by the Murteree Shale. Unconformably overlain by the Toolachee Formation.|Comprises a very widespread, upward fining, interbedded sandstone, siltstone, mudstone and coal succession.|17-JUL-14
14936|Patchawarra Formation|69019|6|Mentioned|p146.|Permian|Permian|Partial erosion of lower levels and evidence of stream rejuvenation in middle levels suggest structural movements in the Cooper Basin in the Early Permian.||||||
14936|Patchawarra Formation|69023|3|Fully described|p79, p81, p82 Fig.18, p83-85, p150|Permian|Permian|See also p163, p191-192. Cooper Basin. Of Kapel (1972). Oil and gas reserves. Peat swamp and flood-plain facies. Thickness from >42 to ~285m. Early Permian. Tectonism discussed. Stratigraphic wells intersection data.||Unit in Gidgealpa Group.||Overlies Merrimelia Formation and Tirrawarra Sandstone. Is overlain by Hutton Sandstone, Epsilon Formation and conformably by Murteree Shale.|Grey, buff or brown, fine- to medium-grained, locally coarse-grained and pebbly, sandstone; grey-brown to dark grey siltstone and mudstone, thinly bedded or laminated; inertinite-rich coal laminations, thin seams and beds, locally 16m thick in the N.|
14936|Patchawarra Formation|69454|5|Briefly described|p38:4, 6, 13|Cisuralian|Cisuralian|Cooper Basin. Potential seal for underlying Tirrawarra Sandstone reservoirs.||Gidgealpa Group.||Lateral equivalent of Purni Formation.||12-JUL-16
14936|Patchawarra Formation|69594|5|Briefly described|p524|||Cooper Basin.||||Is overlain unconformably by Poolowanna Formation.||
14936|Patchawarra Formation|69673|6|Mentioned|p151, p153 fig 125|||||Gidgealpa Group||Overlain by Murteree Shale, Epsilon Formation, overlies Tirrawarra Sandstone||
14936|Patchawarra Formation|69728|6|Mentioned|p285|||Cooper Basin.||Gidgealpa Group.||||
14936|Patchawarra Formation|69797|5|Briefly described|p16, p17 Fig.2|Early Permian|Early Permian|Coal and carbonaceous shale of Patchawarra Formation represent principal source rocks of Cooper Basin, both in source richness and quality, and overall thickness. Age: Asselian - Artinskian (approximated from figure). Geol. Prov: Cooper Basin.||Gidgealpa Group|||Shales and coals.|17-JAN-17
14936|Patchawarra Formation|69946|5|Briefly described|p9, p36, p45, p54|Artinskian|Asselian|Cooper Basin. Peat swamp and floodplain facies.||Unit in Gidgealpa Group.||Overlies Tirrawarra Sandstone. Is overlain by Murteree Shale.||
14936|Patchawarra Formation|69947|5|Briefly described|p13 Fig.7.2|Permian|Permian|Cooper Basin.||Gidgealpa Group.||||
14936|Patchawarra Formation|69982|5|Briefly described|p15, p44, p65, p72, p87, p91, p94, p102|||See also p106, p108. Cooper Basin. Source rocks for hydrocarbons which have migrated to Warburton Basin units. Brief thin section descriptions.||||||
14936|Patchawarra Formation|70317|6|Mentioned|p33-34, 36|Early Permian|Early Permian|Cooper Basin. Vertical section showing fracture densities.||Gidgealpa Group.||Overlies Tirrawarra Sandstone. Is overlain by Murteree Shale.||
14936|Patchawarra Formation|70823|4|Described|iv, p1-p3, p6, p15, 53-58|Kungurian|Sakmarian|Cooper Basin. Hosts deep, dry coal seam gas. Seismic reflection and outcrop characteristics are briefly discussed. Up to 680m thick but with an average thickness of 130m. Deposited in fluviolacustrine, floodplain and minor deltaic environments. Hosts the most significant gas-condensate reservoirs in the Cooper Basin; these are discussed briefly. See also p25-p27, p38, p40-p41, p51, p61, p66, p70, p72, p78-p80, p82-p83. Age based on palynology APP2.1 - APP3.2.||Gidgealpa Group||Overlies and interfingers with the Tirrawarra Sandstone. Conformably overlain by, or intertongues with the Murteree Shale. Unconformably overlain by the Toolachee Formation.|Interbedded sandstone, siltstone, shale and coal.|22-AUG-18
14936|Patchawarra Formation|70824|4|Described|p1-p3, p5, p7-p9, p14, p18-p20, |Kungurian|Sakmarian|Cooper Basin. Together with the Toolachee Formation these are the richest, thickest and most extensive source rocks. Hosts deep dry coal seam gas. Average thickness up to 130m but in the Nappamerri Trough reaches thicknesses in excess of 680m. Deposited under fluviolacustrine, floodplain and deltaic conditions. Source rock geochemistry and outcrop and areal extent discussed. See also p27 fig 3.7, p28-p33, p48-p59, p66, p84, p108-p110, p113, p122.||||Overlies the Tirrawarra Sandstone. Overlain by the Murteree Shale.|Interbedded sandstone, siltstone, shale and coal. Sandstones are dominantly quartzose, fine to medium-grained and locally coarse-grained.|
14936|Patchawarra Formation|70946|5|Briefly described|p1087, p1089-1091|Permian|Early Permian|Cooper Basin. Hosts shallow and deep dry coal seam gas accumulations. Contains a number of non-marine units. Deposited in peat swamp, fluvio-deltaic and lacustrine environments.||Gidgealpa Group.||Is overlain by Murteree Shale.||08-OCT-18
14936|Patchawarra Formation|71265|5|Briefly described|p589|Kungurian|Sakmarian|Cooper Basin.||Gidgealpa Group.||Overlies Tirrawarra Sandstone. Is overlain by Murteree Shale; locally Epsilon Formation (equivalent).||
14936|Patchawarra Formation|71342|5|Briefly described|Ch5 p3, Ch5 p9, Ch5 p36|Kungurian|Sakmarian|Cooper Basin. Deposited in a peat swamp, fluvio-deltaic, lacustrine or floodplain environment. Palynological zone is given in fig 5.3 Ch5 p36. See also Ch5 p45, Ch5 p54, Ch7 p13, Ch10 tbl 10.1, Ch10 p7-p9, Ch10 p14-p15, Ch10 p17-p20, Ch13 p9.||Gidgealpa Group||Overlies the Tirrawarra Sandstone. Overlain by the Murteree Shale.||
14936|Patchawarra Formation|71701|5|Briefly described|p155, p170|Kungurian|Sakmarian|Cooper Basin.||Gidgealpa Group||Overlies the Tirrawarra Sandstone. Overlain by the Murteree Shale.||
14936|Patchawarra Formation|72297|5|Briefly described|p697, p739, p742|Permian|Permian|Cooper Basin. Contains coal, but at too great a depth for economic extraction. One of the main petroleum source rocks within the Basin; also a reservoir. Also contains the largest reservoired gasfield in QLD, at Stokes.||||||
14936|Patchawarra Formation|72497|6|Mentioned|p13.|||Cooper Basin. Oil and gas in Tirrawarra Sandstone and Merrimelia Formation believed to be sourced from this formation (Taylor et al., 1988).||||Overlies Tirrawarra Sandstone.|Includes coals.|
14936|Patchawarra Formation|73167|5|Briefly described|p662, p664, p677|middle Permian|middle Permian|Cooper Basin. Deposited in cycles of fluvio-deltaic, lacustrine and swamp conditions. Contains gas, hydrocarbon source. Onlap in the middle part is attributed to the NW-SE compressional mid-Permian event. NW-SE striking strike-slip faults terminate in the middle Patchawarra Formation. Referred to as middle Patchawarra Formation p677, and as Middle Patchawarra Formation on p662.|||Moorari Beds, VC Coal [?]||Sandstones, shales and thick coals.|
14936|Patchawarra Formation|73244|5|Briefly described|p83-95|Permian|Permian|Cooper Basin. Gas-rich source rock; most prolific source and reservoir unit in the basin; major exploration target. NMR analysis was conducted to create pseudo-capillary pressure curves. Recurring fluvio-deltaic, lacustrine and swamp conditions.|||||Cycles of sandstone, siltstone and coals that range in thickness from less than 1 m to tens of metres.|
14936|Patchawarra Formation|73251|6|Mentioned|p62|Cisuralian|Cisuralian|Cooper Basin. Lacustrine, fluviodeltaic, and peat swamp depositional environments. Hydrocarbon source rock that contains[?] gas and oil.||Gidgealpa Group||Underlain by Tirrawarra Sandstone. Overlain by Murteree Shale.||
14936|Patchawarra Formation|73343|5|Briefly described|p336-338, p341-345|Permian|Permian|Cooper Basin. Gas-rich and low permeability source rock. [The name Middle Patchawarra Formation appears to be used in reference to a seismic reflector/surface/horizon]. [Article includes a detailed investigation of subsurface fracture networks].|||VC Coal and Moorari Beds.|Underlain by Tirrawarra Formation. Overlain by Epsilon Formation and Murteree Shale.|May include sand, shale, and coal.|
14936|Patchawarra Formation|73479|4|Described|p156-p157, p159-161, p163-166, p178|Permian|Permian|Cooper Basin. Fluvio-deltaic/lacustrine/swamp depositional environment. Gas-rich. Intra-formational on-lapping along paleo-structural highs during deposition. Deposition ended with east to west transgression.|ca 285-260 Ma||VC Coal, Moorari Beds|Overlies Tirrawarra Formation, underlies Epsilon Formation, Murteree Shale|Repeated cycles of thick sandstone, shale, and coal. Finer-grained and more shale-dominated in upper part.|
14936|Patchawarra Formation|73495|5|Briefly described|p497, p499-500, p502-506|Kungurian|Artinskian|Of Kapel (1972). Cooper Basin. New CA-TIMS zircon ages from tuffs ranging between 284.87 +/- 0.07/0.16/0.34 Ma and 277.36 +/- 0.04/0.14/0.33 Ma. Basal contact may represent an unconformity. Contains conventional oil and gas accumulations and unconventional gas in tight sandstones and deep coals. Also underlain by basement. Varies substantially in thickness across the basin up to at least 680 m. Reflects fluvial channels, lakes, floodplains, gentle uplands, and raised mire settings. Several informal subdivision schemes have been proposed. Includes several tuffs between 1 and 8 cm thick.|ca 284.87-277.36 Ma U-Pb CA-TIMS|Gidgealpa Group||Underlain by the Tirrawarra Sandstone and unconformably by Merrimelia Formation. Overlain by Murteree Shale.|Locally coarse-grained and pebbly sandstone, fine- to medium-grained sandstone, siltstone, mudstone and coal beds.|
14939|Paterson Point Limestone|35330|6|Mentioned|p20|||||||||
14939|Paterson Point Limestone|36244|6|Mentioned|p2|||Refers to Morony 1977.||||||
14973|Peake Metamorphics|22629|4|Described|fig1p146,153|Statherian|Statherian|||||||
14973|Peake Metamorphics|23054|4|Described|p8-9,32||Paleoproterozoic|||||||07-NOV-08
14973|Peake Metamorphics|23480|5|Briefly described|p20|||See also page 20 Fig. 1||||||
14973|Peake Metamorphics|23481|5|Briefly described|p19 Fig 1|||Geological Province: Gawler Craton.||||||
14973|Peake Metamorphics|23805|5|Briefly described|p4 Fig. 1|Paleoproterozoic|Paleoproterozoic|Geological Province: Gawler Craton.||||||07-NOV-08
14973|Peake Metamorphics|23818|6|Mentioned|p38 Fig.10|||||||||
14973|Peake Metamorphics|24175|6|Mentioned|p48|||||||||
14973|Peake Metamorphics|24422|6|Mentioned|p84 Fig. 1|Paleoproterozoic|Paleoproterozoic|Geological Province: Gawler Craton.||||||07-NOV-08
14973|Peake Metamorphics|24505|5|Briefly described|p5 Fig. 1|||Geological Province: Gawler Craton.||||||
14973|Peake Metamorphics|24506|5|Briefly described|p16|Paleoproterozoic|Paleoproterozoic|Include metamorphosed sediments and mafic and acid volcanics.  Age: 1780+/-12Ma.  Intruded by Wirriecurrie Granite.   Geological Province: Peake and Denison Inliers.||||||07-NOV-08
14973|Peake Metamorphics|24597|5|Briefly described|p526 Fig. 1|Paleoproterozoic|Paleoproterozoic|Geological Province: Gawler Craton.||||||07-NOV-08
14973|Peake Metamorphics|29840|6|Mentioned|p504|||||||||
14973|Peake Metamorphics|30177|6|Mentioned|p38|||Refers to Thomson(1966).||||||
14973|Peake Metamorphics|31798|4|Described|Fig. 2|||Carpentarian||||||
14973|Peake Metamorphics|33468|6|Mentioned|p205|||||||||
14973|Peake Metamorphics|33828|5|Briefly described|p5|||||||||
14973|Peake Metamorphics|34287|6|Mentioned|p35|||||||||
14973|Peake Metamorphics|34537|5|Briefly described|p39|||||||||
14973|Peake Metamorphics|36733|3|Fully described|p14|||||||||
14973|Peake Metamorphics|37854|6|Mentioned|Table 1|||||||||
14973|Peake Metamorphics|38157|6|Mentioned|Table II|||||||||
14973|Peake Metamorphics|39352|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
14973|Peake Metamorphics|40294|6|Mentioned|Table 2|||||||||
14973|Peake Metamorphics|40644|6|Mentioned|p121|||In the Peake and Denison Inlier.||||||13-AUG-08
14973|Peake Metamorphics|41125|6|Mentioned|p55|||||||||
14973|Peake Metamorphics|41402|5|Briefly described|p39|||||||||
14973|Peake Metamorphics|41403|6|Mentioned|Table 5|||||||||
14973|Peake Metamorphics|42223|6|Mentioned|Fig.2 P36|||||||||
14973|Peake Metamorphics|43052|5|Briefly described|p100|||||||||
14973|Peake Metamorphics|43053|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Metasediments, metavolcanics. Geological Province: Peake Inlier and Denison Inlier.||||||07-NOV-08
14973|Peake Metamorphics|43258|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
14973|Peake Metamorphics|43298|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
14973|Peake Metamorphics|44289|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
14973|Peake Metamorphics|44658|14|Not recorded|map legend||Late Precambrian|Older Precam. (G53-15).||||||
14973|Peake Metamorphics|60515|6|Mentioned|p116 Fig.1 |||||||||
14973|Peake Metamorphics|60953|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Age: 1780Ma. Quartzitic and pelitic paragneiss, rhyolite, basalt.||||||07-NOV-08
14973|Peake Metamorphics|60954|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Magnetic orthoamphibolites and basalts. Geological Province: Gawler Craton.||||||07-NOV-08
14973|Peake Metamorphics|61108|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|Quartzitic and pelitic paragneiss, rhyolite and basalt. Age: 1780 Ma.||||||07-NOV-08
14973|Peake Metamorphics|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
14973|Peake Metamorphics|61522|5|Briefly described|p5 Fig.1|||Geological Province: Gawler Craton.||||||
14973|Peake Metamorphics|61659|6|Mentioned|p30 Fig.1. |Paleoproterozoic|Paleoproterozoic||||||Paragneisses.|
14973|Peake Metamorphics|62641|6|Mentioned|p277 Fig.1.|||||||||
14973|Peake Metamorphics|64130|5|Briefly described| p1380 Fig.2, p1381 |||Northern Gawler Craton. Also includes associated sediments of Peake and Denison Inliers, deposited c. 1790 Ma.|||Includes the Tidnamurkana Volcanics.|||
14973|Peake Metamorphics|64722|6|Mentioned|Fig. 5 p.13|Paleoproterozoic|Paleoproterozoic|Of South Australian Craton.||||||
14973|Peake Metamorphics|64725|6|Mentioned|p58 Fig.2. |||Gawler Craton.||||||
14973|Peake Metamorphics|64726|6|Mentioned|p83 Fig.2.|||||||||
14973|Peake Metamorphics|64739|6|Mentioned|p264 Fig.1. |Paleoproterozoic|Paleoproterozoic|Gawler Craton.||||||
14973|Peake Metamorphics|64744|6|Mentioned|p367.|Statherian|Statherian||1780 Ma.|||||
14973|Peake Metamorphics|65376|5|Briefly described|p8 Fig.1.1, pp227-229.|Paleoproterozoic|Paleoproterozoic|Data suggests felsic intrusions between c.1555 Ma and c.1530 Ma, ie younger than the Hiltaba Suite.|||Includes Baltucoodna Quartzite and Tidnamurkuna Volcanics.||Mildly deformed, predominantly quartzitic sequence with interbedded amygdaloidal basalts and rhyolite, and quartz-chlorite-muscovite schists.|
14973|Peake Metamorphics|65390|5|Briefly described|p11 Fig.1, p13|Statherian|Statherian|Contains Baltucoodna Quartzite,Tidnamurkuna Volcanics and quartz-muscovite schists. Syn-tectonic with 1793 Ma Wirriecurrie Granite.||||||
14973|Peake Metamorphics|65922|6|Mentioned|p13 Fig. 4|||Gawler Craton.||||||
14973|Peake Metamorphics|66302|5|Briefly described|p4 Fig.3, p30, p34, p63|Statherian|Statherian|Peake and Denison Domain, Gawler Craton. Deposited in a shallow marine setting.|ca. 1780 Ma|||Faulted against the Wirriecurrie Granite.|Paragneisses.|
14973|Peake Metamorphics|67181|5|Briefly described|p617|Statherian|Statherian|Gawler Craton. Interlayered with Tidnamurkuna Volcanics (Fanning et al. 2007)|ca 1790-1770 Ma||||Includes sedimentary units|
14973|Peake Metamorphics|67323|5|Briefly described|Eastern Australia Time-Space Plot; p31|||Peake and Denison Inliers, Gawler Craton.|~1790-1760 Ma protolith deposition.|||||
14973|Peake Metamorphics|67536|6|Mentioned|Map Legend|||Gawler Craton.|||||Magnetic orthoamphibolite and metabasalt.|
14973|Peake Metamorphics|68131|5|Briefly described|p2 Fig.1|Paleoproterozoic|Paleoproterozoic||||||Metasediments and felsic and mafic volcanics.|
14973|Peake Metamorphics|69004|6|Mentioned|p18|||Gawler Craton.|||||Paragneisses.|
14973|Peake Metamorphics|69649|6|Mentioned|p6 Fig.4||||||||Includes paragneisses.|23-FEB-15
14973|Peake Metamorphics|71318|5|Briefly described|p19|||Geological province: Gawler Craton.||||In shearred contact with WirricurrIe Granite.||
14973|Peake Metamorphics|71348|5|Briefly described|p200,212|Paleoproterozoic|Paleoproterozoic|Geological province: Gawler Craton.|c. 1800-1780 Ma||Includes Tidnamurkuna Volcanics.||Quartz-chlorite-muscovite schists|
14973|Peake Metamorphics|71536|6|Mentioned|p30|||Peake and Denison Inliers.||||||
14994|Pebble Point Formation|12781|6|Mentioned|p386|Paleocene|Paleocene|Otway Basin. Maximum thickness 90m.||Wangerip Group.||Overlies Paaratte Formation conformably and Timboon Sandstone unconformably. Is overlain by Pember Mudstone.||
14994|Pebble Point Formation|12796|5|Briefly described|p456 Fig. 2|Thanetian|Danian|Informally divided into Upper and Lower Pebble Point Formation. Overlies Massacre Shale; underlies Pember Mudstone. Geological Province: Otway Basin.||||||
14994|Pebble Point Formation|22587|6|Mentioned|p79 Fig.7|Middle Miocene|Late Paleocene|||||||
14994|Pebble Point Formation|22674|5|Briefly described|Fig.2 p719|Early Paleocene|Maastrichtian|||||||
14994|Pebble Point Formation|22875|5|Briefly described|p14|Late Paleocene|Late Cretaceous|Of the Wangerrip Group.||||||30-JAN-07
14994|Pebble Point Formation|22944|5|Briefly described|Fig3|Paleocene|Paleocene|||||||
14994|Pebble Point Formation|23230|4|Described|Table4-1p40, 41|Paleocene||||||||
14994|Pebble Point Formation|23307|5|Briefly described|Map Legend|Paleocene|Paleocene|Of Wangerrip Group.||||||24-JUL-08
14994|Pebble Point Formation|23322|5|Briefly described|957 Fig.2|Eocene|Paleocene|Of the Wangerrip Group. Geological Province: Gambier Basin.||||||07-SEP-09
14994|Pebble Point Formation|23671|6|Mentioned|p2|Paleocene|Paleocene|||||||
14994|Pebble Point Formation|23768|6|Mentioned|p14, p19|Paleocene|Paleocene|See also p22, and p37.||||||
14994|Pebble Point Formation|23778|6|Mentioned|p668|||Geological Province: Otway Basin.||||||
14994|Pebble Point Formation|24038|5|Briefly described|p439 Fig.2|Paleocene|Paleocene|Geological Province: Torquay Basin||||||
14994|Pebble Point Formation|24056|5|Briefly described|p85|Paleocene|Paleocene|Of Wangerrip Group. Geological Basin: Otway Basin.||||||24-JUL-08
14994|Pebble Point Formation|24202|5|Briefly described|p313 Fig. 2|Late Paleocene|Early Paleocene|Of the Wangerrip Group. Geological Province: Gambier Sub-basin.||||||24-JUL-08
14994|Pebble Point Formation|24314|5|Briefly described|p61 Fig.2|Paleocene||Geological Province: Otway Basin. Max. Thickness 90m. Of the Wangerrip Group.||||||30-NOV-04
14994|Pebble Point Formation|24455|5|Briefly described|p327|Late Paleocene|Paleocene|Contains fossil molluscs. Conformably overlain by Dilwyn Formation;  transgressively overlaps the Otway Group. Age is Middle Paleocene to Late Paleocene. Geological Province: Otway Basin. See also p321 Fig. 1.||||||24-JUL-08
14994|Pebble Point Formation|24551|5|Briefly described|p246, 292 Fig. 10.3|Paleocene|Paleocene|Of the Wangerrip Group.||||||
14994|Pebble Point Formation|24562|5|Briefly described|p8 Fig. 2|Paleocene|Paleocene|Of the Wangerrip Group. Geological Province: Otway Basin.||||||24-JUL-08
14994|Pebble Point Formation|29355|6|Mentioned|p185|||||||||
14994|Pebble Point Formation|29823|6|Mentioned|p14|||||||||
14994|Pebble Point Formation|29856|6|Mentioned|p40|||||||||
14994|Pebble Point Formation|30244|6|Mentioned|p153|||Palaeocene age||||||
14994|Pebble Point Formation|30454|6|Mentioned|Fig.1|||||||||
14994|Pebble Point Formation|30576|5|Briefly described|Table 2|||||||||
14994|Pebble Point Formation|30578|4|Described|p8|||||||||
14994|Pebble Point Formation|30675|5|Briefly described|p253|||Lithology and radioactivity.||||||24-JUL-08
14994|Pebble Point Formation|30905|6|Mentioned|p149|||||||||
14994|Pebble Point Formation|30932|6|Mentioned|Map legend|Paleocene|Paleocene|Equivalent to Bahgallah Formation. Part of Wangerrip Group.||||||
14994|Pebble Point Formation|31036|1|Redefined|p207|Tertiary|Tertiary|See also p194, Table 9-1.||||||30-JAN-07
14994|Pebble Point Formation|31245|6|Mentioned|p68|||M. Palaeocene. Fauna. Wangerrip Gp.||||||
14994|Pebble Point Formation|31246|6|Mentioned|p54|||Palaeocene||||||
14994|Pebble Point Formation|31372|6|Mentioned|p2|||See also p9.||||||30-JAN-07
14994|Pebble Point Formation|31424|4|Described|p17|||See also p7. Described from core.||||||30-JAN-07
14994|Pebble Point Formation|31514|6|Mentioned|p44|||Shown on Table. Refers McGowran (1965).||||||
14994|Pebble Point Formation|31534|6|Mentioned|p363|||See also Table 19-3||||||
14994|Pebble Point Formation|31624|6|Mentioned|p99|||M.Palaeocene. Synonymous with Bahgallah Fm.||||||
14994|Pebble Point Formation|31625|6|Mentioned|Fig. 5.2|||Palaeocene||||||
14994|Pebble Point Formation|31714|6|Mentioned|p32|||||||||
14994|Pebble Point Formation|31920|6|Mentioned|p55|||M.Palaeocene||||||
14994|Pebble Point Formation|31922|6|Mentioned|Fig.2|||||||||
14994|Pebble Point Formation|32115|4|Described|p1|||See also Fig.1||||||
14994|Pebble Point Formation|32117|6|Mentioned|p84|||||||||
14994|Pebble Point Formation|32120|6|Mentioned|p274|||Palaeocene, fauna||||||
14994|Pebble Point Formation|32344|6|Mentioned|Fig.2|||||||||
14994|Pebble Point Formation|32852|6|Mentioned|p10|||||||||
14994|Pebble Point Formation|32898|6|Mentioned|Table 2-1|||||||||
14994|Pebble Point Formation|33319|6|Mentioned|p167|||Fauna.||||||
14994|Pebble Point Formation|33321|6|Mentioned|p238|||||||||
14994|Pebble Point Formation|33412|6|Mentioned|p218|||M.Palaeocene.||||||
14994|Pebble Point Formation|33940|6|Mentioned|p414|||||||||
14994|Pebble Point Formation|34063|6|Mentioned|p2|||Paleocene. Table||||||
14994|Pebble Point Formation|34172|6|Mentioned|p55|||||||||
14994|Pebble Point Formation|34343|5|Briefly described|p96|||Middle Paleocene||||||
14994|Pebble Point Formation|34987|6|Mentioned|p170|||||||||
14994|Pebble Point Formation|34988|6|Mentioned|Table 9.4|||||||||
14994|Pebble Point Formation|35066|3|Fully described|p203|||||||||
14994|Pebble Point Formation|35285|6|Mentioned|p414|||||||||
14994|Pebble Point Formation|36305|6|Mentioned|p358|||||||||
14994|Pebble Point Formation|36366|3|Fully described|p1|||||||||
14994|Pebble Point Formation|36913|6|Mentioned|p81|||||||||
14994|Pebble Point Formation|37062|6|Mentioned|p179|||||||||
14994|Pebble Point Formation|37548|6|Mentioned|p129|||||||||
14994|Pebble Point Formation|38221|6|Mentioned|p348|||||||||
14994|Pebble Point Formation|38625|6|Mentioned|Table 2|||||||||
14994|Pebble Point Formation|38738|6|Mentioned|p263|||||||||
14994|Pebble Point Formation|40003|5|Briefly described|p44|||See also Fig.10||||||
14994|Pebble Point Formation|40560|6|Mentioned|p4|||||||||
14994|Pebble Point Formation|41016|5|Briefly described|Table 1|||||||||
14994|Pebble Point Formation|41043|6|Mentioned|p95|||||||||
14994|Pebble Point Formation|41075|6|Mentioned|p11|||||||||
14994|Pebble Point Formation|41185|6|Mentioned|p178|||||||||
14994|Pebble Point Formation|41230|6|Mentioned|p127|||||||||
14994|Pebble Point Formation|41269|5|Briefly described|p246|||||||||
14994|Pebble Point Formation|41642|6|Mentioned|p219|||||||||
14994|Pebble Point Formation|41701|6|Mentioned|Map legend|Eocene||||||||
14994|Pebble Point Formation|41704|6|Mentioned|Fig.3|||||||||
14994|Pebble Point Formation|41714|6|Mentioned|p301|||||||||
14994|Pebble Point Formation|41726|5|Briefly described|p421|||||||||
14994|Pebble Point Formation|41769|4|Described|p18|||||||||
14994|Pebble Point Formation|41868|4|Described|p534|||||||||
14994|Pebble Point Formation|42079|6|Mentioned|Fig.2 P264|||||||||
14994|Pebble Point Formation|42152|5|Briefly described|p15|||||||||
14994|Pebble Point Formation|42318|5|Briefly described|p8|||||||||
14994|Pebble Point Formation|42361|6|Mentioned|p17|||||||||
14994|Pebble Point Formation|42453|6|Mentioned|p11|||Port Campbell Embayment||||||
14994|Pebble Point Formation|42524|5|Briefly described|Fig.3 P27|||||||||
14994|Pebble Point Formation|42555|5|Briefly described|Fig.2 P285|||||||||
14994|Pebble Point Formation|42599|6|Mentioned|p618|||||||||
14994|Pebble Point Formation|42827|4|Described|p277|||see also Fig 8.7||||||
14994|Pebble Point Formation|42863|5|Briefly described|Fig.14|||Variation on Victorian unit.||||||
14994|Pebble Point Formation|43052|5|Briefly described|Table 2.1|||||||||
14994|Pebble Point Formation|43171|6|Mentioned|5-8|||Of Wangerrip Group. Age: 55-65Ma||||||
14994|Pebble Point Formation|43195|5|Briefly described|Map Legend|Eocene|Paleocene|See also commentary on back of map. Of Wangerrip Group.||||||
14994|Pebble Point Formation|43208|5|Briefly described|map legend|Late Paleocene|Maastrichtian|Of Maastrichtian - Late Palaeocene age. Of Wangerrip Group.||||||24-JUL-08
14994|Pebble Point Formation|43219|5|Briefly described|Fig.3,p6.|Paleocene|Maastrichtian|Of Wangerrip Group.||||||30-JAN-07
14994|Pebble Point Formation|43493|6|Mentioned|32||Tertiary|||||||
14994|Pebble Point Formation|43590|14|Not recorded|p16|Paleocene|Late Cretaceous|||||||
14994|Pebble Point Formation|43660|6|Mentioned|Fig.6,p15||Paleocene|||||||
14994|Pebble Point Formation|43733|6|Mentioned|Fig.2.11,p65||Paleocene|||||||
14994|Pebble Point Formation|43744|6|Mentioned|Fig.3,p3|||||||||
14994|Pebble Point Formation|43814|6|Mentioned|Fig.3,p115|||||||||
14994|Pebble Point Formation|43937|5|Briefly described|Map Legend|Paleocene|Santonian|||||||
14994|Pebble Point Formation|44133|4|Described|p154|Early Eocene|Late Paleocene|Of the Wangerrip Group. Geological Province: Gambier Basin. Unconformably overlies Sherbrook Group. Thickness: 40m.||||||30-JAN-07
14994|Pebble Point Formation|44677|14|Not recorded|p6|||Amosopollis.||||||
14994|Pebble Point Formation|47054|6|Mentioned|p491|||||||||
14994|Pebble Point Formation|48581|14|Not recorded|p14|||||||||
14994|Pebble Point Formation|48911|3|Fully described|p23|||Middle - Upper Palaeocene.||||||
14994|Pebble Point Formation|48977|6|Mentioned|Fig.5|||||||||
14994|Pebble Point Formation|60538|5|Briefly described|p474 Fig. 13|||Geological Province: Otway Basin.||||||
14994|Pebble Point Formation|60563|5|Briefly described|p45 Fig. 1, p46|||Estuarine channel sandstones. Overlain by the Pember Mudstone Member of the Dilwyn Formation.||||||16-JUN-05
14994|Pebble Point Formation|60599|5|Briefly described|p84|Late Cretaceous|Late Cretaceous|Of the Wangerrip Group. Geological Province:Otway  Basin.||||||
14994|Pebble Point Formation|61016|6|Mentioned|p13|||See also Pebble Point formation. Geological Province: Otway Basin.||||||20-APR-05
14994|Pebble Point Formation|61017|5|Briefly described|p5|Selandian|Danian|Of the Wangerrip Group. Geological Province: Otway Basin.||||||07-FEB-11
14994|Pebble Point Formation|61155|5|Briefly described|p2, p18|Early Paleocene|Early Paleocene|Paralic to shallow-marine iron-rich oolitic sediments.Overlain by Eastern View and Dilwyn Formations and by Pember Mudstone. Overlies Timboon Sand Member (Sherbrook Group). Max. thickness: 150m. Geological Province: Otway Basin, Torquay Basin.||||||30-JAN-07
14994|Pebble Point Formation|61182|3|Fully described|p19-20, p32, p89|Maastrichtian|Maastrichtian|Of Wangerrip Gp. Overlies Eumeralla Fm; disconform.on Timboon Sand Member (Paaratte Fm) in west. Capped by Pember Mudstone. Grades lat. into Moomowroong Sand. Max.thick:158m. Geol.Prov:Otway Basin. Moomowroong Sand, Wiridjil Gravel = lateral equivs.||||||
14994|Pebble Point Formation|61185|5|Briefly described|p57|Tertiary|Tertiary|Of the Wangerrip Group. Contain large river-rounded lithic cobbles. Age: ~65Ma. Geol. Prov: Otway Basin.||||||07-FEB-11
14994|Pebble Point Formation|61470|5|Briefly described|p28 Fig. 5|Selandian|Danian|Of the Wangerrip Group. Overlain by and interfingered with Pember Mudstone.  Geological Province: Otway Basin.||||||12-OCT-05
14994|Pebble Point Formation|61547|6|Mentioned|p461 Fig.2. |Paleocene|Paleocene|||Unit in Wangerrip Group.||Overlies Paaratte Formation and Timboon Sandstone.||
14994|Pebble Point Formation|61622|5|Briefly described|p436 Fig. 2|Paleocene|Paleocene|Of Wangerrip Group. Geological Province: Otway Basin.||||||07-FEB-11
14994|Pebble Point Formation|61623|6|Mentioned|p449 Fig. 4|Paleocene|Paleocene|Of Wangerrip Group. Geological Province: Otway Basin.||||||07-APR-09
14994|Pebble Point Formation|61626|5|Briefly described|p486, p486 Fig. 2, p488 Fig. 4|Paleocene|Paleocene|Of Wangerrip Group. Geological Province: Otway Basin.||||||07-APR-09
14994|Pebble Point Formation|61627|5|Briefly described|p500 Fig. 2|Paleocene|Paleocene|Of Wangerrip Group. Overlian by Pember Mudstone. Geological Province: Otway Basin.||||||07-FEB-11
14994|Pebble Point Formation|61628|5|Briefly described|p509 Fig. 3|Paleocene|Paleocene|Of Wangerrip Group. Geological Province: Otway Basin.||||||07-APR-09
14994|Pebble Point Formation|62896|5|Briefly described|p88|Late Paleocene|Late Paleocene|Geological Province: Otway Basin.||||||07-FEB-11
14994|Pebble Point Formation|63122|5|Briefly described|p17 Fig. 4.3|Late Paleocene|Early Paleocene|Of the Wangerrip Group. Max. thickness: 90m. Geological Province: Otway Basin.||||||
14994|Pebble Point Formation|63124|3|Fully described|p49 Fig. 5.2, p87 Fig. 5.29, p88|Early Eocene|Late Paleocene|Previously referred to as Bahgallah Formation in South Australia. Of the Wangerrip Group. Unconformable on Sherbrook Group; conformably overlain by Pember Mudstone. Age: 55-51Ma. Max. thickness: 90m. Geological Province: Otway Basin.||||||
14994|Pebble Point Formation|63129|5|Briefly described|p137|Early Tertiary|Early Tertiary|Geological Province: Otway Basin. May act as a regional seal, and together with Pember Mudstone is the only seal for the condensed Sherbrook Group.||||||
14994|Pebble Point Formation|63130|5|Briefly described|p143|||Geological Province: Otway Basin.||||||04-FEB-08
14994|Pebble Point Formation|63269|5|Briefly described|p605-607|Paleocene|Paleocene|Otway Basin. Contains a marginally-mature oil stain thought to be sourced from Sherbrook Group. Details of oils and oil stains in named wells tabulated.||Wangerrip Group.||||
14994|Pebble Point Formation|63431|5|Briefly described|p677 Fig. 2|Paleocene|Paleocene|Basal unit of the Wangerrip Group. Geological Province: Penola Trough/Otway Basin.||||||07-FEB-11
14994|Pebble Point Formation|63740|5|Briefly described|p88, p92|Paleocene|Paleocene|Geological province: Otway Basin.||||||07-FEB-11
14994|Pebble Point Formation|66002|5|Briefly described|p10 Tb.7, p10 Tb.8|Paleogene|Paleogene|Of Wangerrip Group. Defined by Tickell et al 1992.||||||
14994|Pebble Point Formation|66245|5|Briefly described|p6 Fig.5. |Selandian|Danian|||Unit in Wangerrip Group.||Is overlain by Pember Mudstone.||
14994|Pebble Point Formation|67061|5|Briefly described|p545, p546 Fig.3.|Paleocene|Paleocene|Otway Basin. Coal measures and underlying mudstones and sandstones in this unit have sedimentological and stratigraphic affinities with similar facies in onshore Eastern View Group (Torquay Sub-basin).||Unit in Wangerrip Group.||||
14994|Pebble Point Formation|67366|5|Briefly described|p103 Fig.2. |Paleocene|Paleocene|||Unit in Wangerrip Group.||Overlies Massacre Shale. Is overlain by Pember Mudstone.|Shallow to nearshore marine sandstone and shale.|
14994|Pebble Point Formation|67367|5|Briefly described|p131 Fig.2, pp132-133. |Late Paleocene|Early Paleocene|Contains oils derived from terrestrial, land-plant material; subjected to extensive microbial alteration and water washing.||Unit in Wangerrip Group.||||
14994|Pebble Point Formation|68116|5|Briefly described|Appendix, Maps 54-55.|Paleocene|Paleocene||||||Quartz sand, minor clay: micaceous, fine-grained, friable, generally massive; minor planar cross-bedding; minor gravel, minor volcanic and metamorphic lithic cobbles and pebbles; near shore, shallow marine deposits.|
14994|Pebble Point Formation|69297|5|Briefly described|p79|Thanetian|Maastrichtian|Otway Basin. See Pebble Point Formation, Lower and Upper.||Wangerrip Group||Overlies the Timboon Sandstone and the Massacre Shale. Overlain by the Dilwyn Formation.||
14994|Pebble Point Formation|69651|5|Briefly described|p10|Paleocene|Paleocene|||Wangerrip, Nirranda Groups [?].||Abuts Eastern View Formation. Is overlain by Pember Mudstone.||
14994|Pebble Point Formation|70077|5|Briefly described|Nelson: Fig.2. Regional: Fig.4; p5, p7-8|Paleocene|Paleocene|Otway Basin. Shallow marine to coastal depositional environments. An Austral 2 Petroleum System oil show, in Wilson 1, was possibly sourced from Belfast Mudstone. Is sealed by Pember Mudstone.||Wangerrip Group.||Overlies Massacre Shale or Timboon Sandstone. Is overlain by Pember Mudstone.||
14994|Pebble Point Formation|70078|5|Briefly described|Northern: Fig.2. Regional: Fig.4|Paleocene|Paleocene|Gambier Embayment and Voluta Trough.||Wangerrip Group.||Overlies Massacre Shale. Is overlain by Pember Mudstone.||
14994|Pebble Point Formation|70193|6|Mentioned|p285 fig 3|||See also p284 Fig 2 where informally divided into upper and lower parts.||||||
14994|Pebble Point Formation|70880|6|Mentioned|p77|Paleocene|Maastrichtian|Otway Basin.||||||
14994|Pebble Point Formation|71266|6|Mentioned|p614 Fig.3|Paleocene|Late Cretaceous|Otway Basin.||||||
14994|Pebble Point Formation|71437|4|Described|Fig. 1 opp 154,  p155, p158-159|Paleocene|Paleocene|Important marker horizon heralding onset of neritic marine conditions. Compared with Flaxman Formation.||Of Wangerrip Group.||Transitional with Pember Mudstone Member of Dilwyn Formation.|Glauconitic sandy dolomite, sand and gravel, minor conglomerate and mudstone.|
14994|Pebble Point Formation|73357|5|Briefly described|p25-26, p44, p46, p48|Thanetian|Danian|Otway Basin. Correlated with multiple biozones including Lygistepollenites balmei Spore-Pollen Zone, typically marginal to nearshore marine depositional environments. Lower part coincides with Alisocysta circumtabulata Dinocyst Zone.||Of Wangerrip Group?||Overlies K/Pg Boundary Shale, underlies Pember Mudstone.||
14994|Pebble Point Formation|73383|5|Briefly described|p3, p10 Tb.3.7, p21, p24, p27, p265-266|Paleocene|Paleocene|Otway Basin. Equivalent to chemostratigraphic package S5-P8 continaing high Th/K, Fe and P values. Lithologies based on geochemistry using the ChemLith classification include argillaceous and calcareous sandstones, limestone, calcareous limestone, and mudstone; and using the Herron classification (1988) includes quartz arenite, Fe-shale, Fe-sand, sublith-arenite. See also vi, p11 Tb.3.9, p66-67, p83, p118-119, p131, p138-140, p199, p214, p247, p258.||Wangerrip Group||Overlies Sherbrook Group, underlies Pember Mudstone|Sandstones. Can be oolitic in parts and contains fossiliferous material.|
14994|Pebble Point Formation|73385|5|Briefly described|p5|Paleocene|Paleocene|Otway Basin.||Wangerrip Group||Overlies Sherbrook Group, underlies Pember Mudstone.|Shallow marine and nearshore sandstones.|
14994|Pebble Point Formation|73386|4|Described|p4, p6, p12, Attachment A1|Paleocene|Paleocene|Otway Basin. Deposited during a regression, forming a lowstand-transgressive systems tract, resulting in a blanket of marginal marine beach and inner shelf sandstones. Downlapped by a strongly prograding series of deltaic sequences dominated by the landward Dilwyn Formation facies and basinward Pember Mudstone facies. Onshore, the formation is thin with a sheet-like geometry, fines upwards into Pember Mudstone. Occurs within the Lower Lygistepollenites balmei Spore-Pollen Subzone.||Wangerrip Group||Overlies Cretaceous/Paleogene boundary shale, underlies Pember Mudstone|Consists of carbonaceous sandy claystones, granule conglomerate and fine to coarse-grained quartz sandstone.|
14994|Pebble Point Formation|73594|5|Briefly described|p4, p45 Fig.5.19|Paleocene|Paleocene|Otway Basin.||Wangerrip Group||Underlies Pember Mudstone|Shallow marine and nearshore sandstones.|
15008|Peela Conglomerate Member|22629|5|Briefly described|p158|||||||||
15008|Peela Conglomerate Member|23490|6|Mentioned|p22|||Of Tarcoola Formation. Renamed Mentor Formation.||||||
15008|Peela Conglomerate Member|39905|6|Mentioned|Fig.4|||||||||
15008|Peela Conglomerate Member|40910|6|Mentioned|p11|||||||||
15008|Peela Conglomerate Member|41995|5|Briefly described|p12|||||||||
15008|Peela Conglomerate Member|42469|5|Briefly described|p13, p17|||||||||
15008|Peela Conglomerate Member|43052|4|Described|p68|||of Tarcoola Formation||||||
15008|Peela Conglomerate Member|44935|5|Briefly described|Map Legend||Proterozoic|||||||
15008|Peela Conglomerate Member|50605|5|Briefly described|p8.6|||Of the Tarcoola Formation. Geological Province: Gawler Craton & Curnamona Province.||||||
15008|Peela Conglomerate Member|63276|5|Briefly described|p3 Fig. 2, p14 Fig. 3|Proterozoic|Proterozoic|Basal unit of the Tarcoola Formation. See also p5 Fig. 4.||||||
15008|Peela Conglomerate Member|64137|5|Briefly described|p1543 Fig.2, p1544, p1545 Fig.4 |Paleoproterozoic|Paleoproterozoic|||Of the Tarcoola Formation.|||Pink arkosic fluvial grit, with locally abundant banded iron formation fragments|
15008|Peela Conglomerate Member|66302|6|Mentioned|p23, p32|Statherian|Statherian|Wilgena Domain, Gawler Craton. Deposited in a fluvial to marginal marine setting. Contains detrital zircons dated at 1733 +/- 5 Ma to 1715 +/- 8 Ma.  Also misspelt as the Peela Conglomerate on p23.||Tarcoola Formation||Overlain by the Fabian Quartzite Member.|Basal conglomerate.|
15047|Pepegoona Porphyry|22631|6|Mentioned|p176|Calymmian|Calymmian|1575-1580Ma||||||
15047|Pepegoona Porphyry|23394|5|Briefly described|Map legend|Proterozoic|Proterozoic|||||||
15047|Pepegoona Porphyry|23411|6|Mentioned|Map Legend|||||||||
15047|Pepegoona Porphyry|23818|5|Briefly described|p35|Statherian|Statherian|Of the Brindana Schist. Age: 1650 Ma.||||||18-APR-05
15047|Pepegoona Porphyry|24176|4|Described|p7, p26 Tb. 1|Proterozoic|Proterozoic|Of Radium Creek Metamorphics.  ?Recrystallised rhyolite.  Max. thickness: >550m.  Geological Province: Mount Painter Province.||||||
15047|Pepegoona Porphyry|29840|6|Mentioned|Fig.3|||||||||
15047|Pepegoona Porphyry|30177|4|Described|p33|||||||||
15047|Pepegoona Porphyry|30807|6|Mentioned|p103|||Suggested map symbol||||||
15047|Pepegoona Porphyry|30920|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Prob.Lower Proterozoic||||||07-NOV-08
15047|Pepegoona Porphyry|34537|6|Mentioned|p35|||||||||
15047|Pepegoona Porphyry|36733|6|Mentioned|p21|||||||||
15047|Pepegoona Porphyry|39352|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
15047|Pepegoona Porphyry|41402|6|Mentioned|p38|||||||||
15047|Pepegoona Porphyry|42624|5|Briefly described|p30|||||||||
15047|Pepegoona Porphyry|43052|5|Briefly described|p151|||Of Coats & Blissett, 1971.||||||
15047|Pepegoona Porphyry|48894|6|Mentioned|p64|||||||||
15047|Pepegoona Porphyry|50605|5|Briefly described|p10.4|||Geological Province: Gawler Craton & Curnamona Province.||||||
15047|Pepegoona Porphyry|60953|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Felsic porphyry.||||||
15047|Pepegoona Porphyry|61108|5|Briefly described|map legend|Mesoproterozoic|Mesoproterozoic|Felsic porphyry.||||||
15047|Pepegoona Porphyry|61556|14|Not recorded|p10|Carpentarian|Carpentarian|||||||
15047|Pepegoona Porphyry|63866|6|Mentioned|p43|||||||||
15047|Pepegoona Porphyry|66302|6|Mentioned|p49, p78||||ca. 1585-1575 Ma|||||
15047|Pepegoona Porphyry|67536|6|Mentioned|Map Legend|||Curnamona Province. Mapped with Petermorra Volcanics as M39.|||||Dacite to rhyolite and volcaniclastic and epiclastic rocks; rhyolitic to rhyodacitic metavolcanic rock|
15047|Pepegoona Porphyry|67540|1|Redefined|p34, 25-28: Fig.1, Tb.1, 2; p36 Tb.3|Calymmian|Statherian|Named after Pepegoona Well. Type locality: Pepegoona Gorge SW of Mount Neill. Curnamona Province: Moolawatana Domain. Definition reference: this article, and Fricke and Hore (2011). Is considered to be an extrusive equivalent of Mount Neill Granite. Age references: the older by LA-ICP-MS (Kromkhun, 2010); the younger by SHRIMP (Jagodzinski and Hore, in prep.)|1603 +/- 19 Ma and 1582 +/- 3 Ma.|Of the Ninnerie Supersuite.||In faulted contact with the Brindana Schist. Intruded by the Mount Neill Granite.|Aphanitic 'rhyolitic' groundmass containing lightly scattered small- to medium-size phenocrysts, mainly of potash feldspar, less commonly of quartz and plagioclase.|25-NOV-22
15047|Pepegoona Porphyry|67653|6|Mentioned|p4|||Geological province: Curnamona Province.||||||
15047|Pepegoona Porphyry|68126|6|Mentioned|p6|Mesoproterozoic|Mesoproterozoic|Mount Painter Inlier, Curnamona Province.||||||
15047|Pepegoona Porphyry|69019|6|Mentioned|p14.|||Mapping by Teale (1993) suggests that Pepegoona Porphyry and Freeling Heights Quartzite are not part of Radium Creek Metamorphics.||||||
15047|Pepegoona Porphyry|69023|6|Mentioned|p14|||Formerly part of Radium Creek Metamorphics.||||||
15047|Pepegoona Porphyry|69562|5|Briefly described|p671 Tb.5||||1576 +/- 2 Ma (Teale and Flint, 1993).||||Rhyolitic and rhyodacitic metavolcanics.|
15047|Pepegoona Porphyry|69650|2|Defined|p4 Tb.1, p2, p9, p11, p13, p62, p64, p68|Calymmian|Statherian|See also p70-75. Campana et al. (1961). Named after Pepegoona Well, near Moolawatana Homestead. Type locality: Excellent exposures of the Pepegoona Porphyry are found in the Pepegoona Gorge, GDA 94, 365320 mE, 6671400 mN, along a SSE trending creek towards the plains at Pepegoona Well . This section displays subsequent sodic alteration, shear zones and columnar jointing and flow banding (Coats and Blissett, 1971). Moolawatana Domain, Curnamona Province. Is spatially related to (i.e. appears to be intruded by) Mount Neill Granite and is regarded by various authors (named) as an extrusive of that unit. Geochronology, geochemistry detailed. Has been albitised in several areas.|1603 +/- 19 Ma U-Pb zircon, Kromkhun (2010).|Unit in Ninnerie Supersuite.||Underlies Brindana Schist (tectonic contact, not conformably).|Aphanitic rhyolitic groundmass containing lightly scattered small- to medium-sized phenocrysts, mainly of K-feldspar, less commonly quartz and plagioclase. A-type.|25-NOV-22
15047|Pepegoona Porphyry|69654|6|Mentioned|p3|||Curnamona Province.||||||
15047|Pepegoona Porphyry|70384|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Another age is given: 1603 +/- 19 Ma (ICPMS).|1582 +/- 4 Ma (SHRIMP U-Pb zircon).|Ninnerie Supersuite.|||Feldspar porphyry, green, coarse-grained.|
15047|Pepegoona Porphyry|71531|14|Not recorded|p8, 9, 11|||Refer to Campana et al, 1961.||||||
15047|Pepegoona Porphyry|72454|6|Mentioned|p2 Fig.2|Mesoproterozoic|Mesoproterozoic|Part of Mount Painter Inlier.  Shown only on p2 Fig.2.|||||Includes porphyry.|
15047|Pepegoona Porphyry|72456|6|Mentioned|Solid Geology Interpretation|||||||||
15047|Pepegoona Porphyry|72949|6|Mentioned|p36|Calymmian|Statherian|Curnamona Province. Mount Painter.|1603-1582 Ma|||||
15047|Pepegoona Porphyry|73251|6|Mentioned|p36|Calymmian|Calymmian|Curnamona Province, Mount Painter and Mount Babbage inliers. Includes uraniferous crystalline rock.|c. 1580 Ma|||||
15067|Permano Adamellite|30923|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
15067|Permano Adamellite|31965|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
15067|Permano Adamellite|43052|6|Mentioned|p162|||||||||
15067|Permano Adamellite|50607|5|Briefly described|p2.2|||Geological Province: Musgrave Block. Of the Southern granites Suite (Kulgera Supersuite).||||||
15067|Permano Adamellite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite|
15067|Permano Adamellite|71268|6|Mentioned|1m_geologyp12_lut.csv|||||Unit of Pitjantjatjara Suite.|||Monzogranite, foliated|
15091|Pertaoorrta Group|1842|5|Briefly described|p3|Early Cambrian|Ediacaran|Of Amadeus Basin.|||Includes Maurice Formation, Sir Frederick Conglomerate, Ellis Sandstone, Mount Currie Conglomerate, Carnegie Formation, Winnall beds, Namatjira Formation, Todd River Dolostone and Arumbera Sandstone.|||
15091|Pertaoorrta Group|9199|5|Briefly described|Map legend|Cambrian|Cambrian|Including undivided rocks of sandstone, siltstone, shale, dolomite, limestone, evaporites.  Geological Province: Amadeus Basin.||||||
15091|Pertaoorrta Group|9814|5|Briefly described|Map Legend|Cambrian|Cambrian|||||||
15091|Pertaoorrta Group|22561|5|Briefly described|p9|||||||||
15091|Pertaoorrta Group|22564|6|Mentioned|p60|Cambrian|Neoproterozoic|||||||
15091|Pertaoorrta Group|22566|4|Described|p76|Late Cambrian|Neoproterozoic|||||||
15091|Pertaoorrta Group|22650|6|Mentioned|Fig 2 on p 157|Cambrian||||||||
15091|Pertaoorrta Group|22651|4|Described|p 173|Cambrian|Neoproterozoic|Five major depositional sequences are recognised in the Pertaoorrta Group and described.||||||17-JUL-13
15091|Pertaoorrta Group|22652|6|Mentioned|p 195|Late Cambrian|Neoproterozoic|||||||
15091|Pertaoorrta Group|22654|6|Mentioned|p 252|||||||||
15091|Pertaoorrta Group|22655|6|Mentioned|p 255|||Informally divided in to upper and lower Pertaoorrta Groups, p255.||||||22-NOV-06
15091|Pertaoorrta Group|22657|6|Mentioned|p 285|||||||||
15091|Pertaoorrta Group|22760|6|Mentioned|p339|||||||||
15091|Pertaoorrta Group|22804|6|Mentioned|p445|Late Cambrian|Neoproterozoic|||||||
15091|Pertaoorrta Group|22807|6|Mentioned|Fig 3 on p495|Late Cambrian|Early Cambrian|||||||
15091|Pertaoorrta Group|22824|6|Mentioned|Fig 7 on p536|||||||||
15091|Pertaoorrta Group|22826|6|Mentioned|Fig 4 on p567|||||||||
15091|Pertaoorrta Group|24063|5|Briefly described|p218 Fig.2|Proterozoic|Proterozoic|Geological Province: Amadeus Basin.||||||
15091|Pertaoorrta Group|24064|5|Briefly described|p229 Fig.7|Cambrian|Cambrian|Geological Province: Amadeus Basin.||||||
15091|Pertaoorrta Group|24111|6|Mentioned|p214 Fig. 9|||Geological Province: Amadeus Basin.||||||30-MAR-05
15091|Pertaoorrta Group|29972|6|Mentioned|Table 1|||||||||
15091|Pertaoorrta Group|30238|4|Described|p64|||Cambrian age||||||
15091|Pertaoorrta Group|30258|6|Mentioned|Fig.2|||Cambrian age||||||
15091|Pertaoorrta Group|31566|6|Mentioned|p230|||Cambrian||||||
15091|Pertaoorrta Group|31707|6|Mentioned|Table 1|||See also Fig. 2||||||
15091|Pertaoorrta Group|31973|6|Mentioned|p3|||Correlation||||||
15091|Pertaoorrta Group|33307|6|Mentioned|Fig.6|||||||||
15091|Pertaoorrta Group|33761|6|Mentioned|p146|||See also Fig.3. Adel.- Camb.||||||
15091|Pertaoorrta Group|33971|6|Mentioned|p28|||Stratigraphic section Fig.15.||||||
15091|Pertaoorrta Group|34111|5|Briefly described|Table 2|||Cambrian. See also pp6,14-19.||||||22-NOV-06
15091|Pertaoorrta Group|34442|5|Briefly described|Table 1, p8,10|||Cambrian||||||03-JUL-17
15091|Pertaoorrta Group|34488|4|Described|Table 1|||See also Table 2. Cambrian||||||
15091|Pertaoorrta Group|34579|4|Described|Table 2|||Cambrian. See also pp15,17, Fig.2.||||||22-NOV-06
15091|Pertaoorrta Group|35102|6|Mentioned|p3|||||||||
15091|Pertaoorrta Group|36473|6|Mentioned|Map legend|Ordovician|Adelaidean|Adelaidean to Ordovician||||||
15091|Pertaoorrta Group|38445|6|Mentioned|p102|||||||||
15091|Pertaoorrta Group|38606|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
15091|Pertaoorrta Group|38885|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
15091|Pertaoorrta Group|39565|6|Mentioned|Fig.14|||||||||
15091|Pertaoorrta Group|39583|6|Mentioned|Map legend|Late Cambrian|Neoproterozoic|Late Cambrian to Late Proterozoic||||||
15091|Pertaoorrta Group|39931|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
15091|Pertaoorrta Group|40740|3|Fully described|p67|||Described p13.||||||22-NOV-06
15091|Pertaoorrta Group|40810|6|Mentioned|p3|||||||||
15091|Pertaoorrta Group|40910|6|Mentioned|p13|||||||||
15091|Pertaoorrta Group|40911|6|Mentioned|Map legend|Cambrian|Cambrian|Prob. Cambrian||||||
15091|Pertaoorrta Group|40998|6|Mentioned|p431|||||||||
15091|Pertaoorrta Group|41018|6|Mentioned|p240|||||||||
15091|Pertaoorrta Group|41039|6|Mentioned|Fig.2|||||||||
15091|Pertaoorrta Group|41115|6|Mentioned|p1400|||||||||
15091|Pertaoorrta Group|41224|6|Mentioned|p430|||||||||
15091|Pertaoorrta Group|41270|6|Mentioned|Table 1|||||||||
15091|Pertaoorrta Group|41385|6|Mentioned|Fig.3|||||||||
15091|Pertaoorrta Group|41621|6|Mentioned|Map legend|Cambrian||||||||
15091|Pertaoorrta Group|41717|6|Mentioned|Fig.2|||||||||
15091|Pertaoorrta Group|41723|6|Mentioned|Map legend|Neoproterozoic|Early Cambrian|||||||
15091|Pertaoorrta Group|41801|5|Briefly described|p212|||||||||
15091|Pertaoorrta Group|41819|6|Mentioned|Map legend|Cambrian||||||||
15091|Pertaoorrta Group|41820|5|Briefly described|p7|||||||||
15091|Pertaoorrta Group|42060|6|Mentioned|Fig.5 P140|||||||||
15091|Pertaoorrta Group|42082|6|Mentioned|Fig.3 P323|||||||||
15091|Pertaoorrta Group|42354|6|Mentioned|p6|||||||||
15091|Pertaoorrta Group|42504|6|Mentioned|Plate 11 P42|||||||||
15091|Pertaoorrta Group|42940|5|Briefly described|Plate 2|Cambrian|Cambrian|Sandstone, siltstone, shale, limestone, dolostone, conglomerate; marine fossils. Age: 590-500Ma.  Geological province: Amadeus Basin.||||||23-JAN-08
15091|Pertaoorrta Group|43035|5|Briefly described|p20|||||||||
15091|Pertaoorrta Group|43225|5|Briefly described|Map Legend||Cambrian|In the Amadeus Basin.||||||22-NOV-06
15091|Pertaoorrta Group|43503|6|Mentioned|32-50|Late Cambrian|Proterozoic|||||||
15091|Pertaoorrta Group|44133|5|Briefly described|p42|||Geological Province: Amadeus Basin.||||||
15091|Pertaoorrta Group|44335|4|Described|p.11||Cambrian|Table 2. p.10.||||||
15091|Pertaoorrta Group|44336|14|Not recorded|map legend||Cambrian|SG/53-3.||||||
15091|Pertaoorrta Group|44342|4|Described|p.5, Table 2||Cambrian|SG/53-5.||||||
15091|Pertaoorrta Group|44343|14|Not recorded|map legend||Cambrian|||||||
15091|Pertaoorrta Group|44393|4|Described|p.3,7,Tb.1||Early Cambrian|L.Cambrian.||||||
15091|Pertaoorrta Group|44394|14|Not recorded|map legend||Cambrian|||||||
15091|Pertaoorrta Group|44395|14|Not recorded|p.8|||Correlates with Cleland Sandstone (Cambrian?).||||||
15091|Pertaoorrta Group|44402|5|Briefly described|map legend||Cambrian|||||||02-DEC-04
15091|Pertaoorrta Group|44433|14|Not recorded|map legend||Cambrian|||||||
15091|Pertaoorrta Group|44484|14|Not recorded|p.10,12,Tb.1,2,Fig.4|||(Cambrian).||||||
15091|Pertaoorrta Group|44485|14|Not recorded|map legend||Cambrian|Includes Quandong Conglomerate, Eninta Sandstone, Chandler Limestone, Tempe Formation, Jay Creek Limestone,  Illara Sandstone, Deception Formation, Petermann Sandstone, Goyder Formation.||||||
15091|Pertaoorrta Group|44495|4|Described|p.6, map||Cambrian|AYERS ROCK sheet (G52-8). See p.8,10, for details.||||||22-NOV-06
15091|Pertaoorrta Group|44496|5|Briefly described|map legend||Cambrian|||||||02-DEC-04
15091|Pertaoorrta Group|44497|4|Described|p.6, Table 1||Cambrian|SF/53-13.||||||
15091|Pertaoorrta Group|44498|14|Not recorded|map legend||Cambrian|||||||
15091|Pertaoorrta Group|44505|14|Not recorded|p.5,7,8, Fig. 1||Cambrian|||||||
15091|Pertaoorrta Group|44506|14|Not recorded|map legend||Cambrian|||||||
15091|Pertaoorrta Group|45036|6|Mentioned|p3|||||||||
15091|Pertaoorrta Group|45041|4|Described|p49|||See also p50-60. Camb.||||||22-NOV-06
15091|Pertaoorrta Group|45170|6|Mentioned|p23|||||||||
15091|Pertaoorrta Group|46730|5|Briefly described|p7|Cambrian|Proterozoic|Overlain by Pacoota Sandstone. Geological Province: Amadeus Basin||||||22-NOV-06
15091|Pertaoorrta Group|46829|6|Mentioned|Fig.2|||||||||
15091|Pertaoorrta Group|46928|6|Mentioned|Table 1|||||||||
15091|Pertaoorrta Group|46957|6|Mentioned|p165|||||||||
15091|Pertaoorrta Group|48639|14|Not recorded|opp.p.1,map|Ordovician|Cambrian|Ord-Cam.||||||
15091|Pertaoorrta Group|48838|1|Redefined|p.14, Tb.1|||||||||
15091|Pertaoorrta Group|48862|14|Not recorded|p.16-24,31|||Now redefined as Pertaoorrta Formation. (F52-15).||||||22-NOV-06
15091|Pertaoorrta Group|48863|2|Defined|p.15||Early Ordovician|Tb.1. opp.p.7,p.5,10,11,16,18,19,26,40-42,Pl.9,10,15,15. Lower Ordovician. (G52-4,G53-1).||||||
15091|Pertaoorrta Group|48864|14|Not recorded|p.32|||Now called Pertaoorrta Formation.||||||
15091|Pertaoorrta Group|48865|2|Defined|p.10,Fig.20||Cambrian|Many figures. Fig.4,11,12,23,42,45,47,49,Fig.14,Pl.7,8. (G53-5,G52-8).||||||
15091|Pertaoorrta Group|48880|14|Not recorded|p.20,33,Pl.10,12,13||Cambrian|(F53-13,15,G53-3).||||||
15091|Pertaoorrta Group|48890|14|Not recorded|p.31,43|||Includes, Todd River Dolomite, Shannon Fm, Jay Ck Lm, Hugh River Shale, Giles Ck - Dolomite, Goyder Fm-, Chandler Ls, Arumbera Sandstone.||||||
15091|Pertaoorrta Group|48963|6|Mentioned|p22|||||||||
15091|Pertaoorrta Group|60547|5|Briefly described|Map Legend|Cambrian|Cambrian|Sandstone, siltstone, shale, dolomite, limestone, evaporites. Geological Province: Amadeus Basin.||||||03-JUN-05
15091|Pertaoorrta Group|60674|5|Briefly described|Map legend|Cambrian|Cambrian|Includes: Cleland Sandstone, Tempe, Illara, Deception and Petermann Formations, Hugh River Shale and the Goyder Formation.  Geological Province: Amadeus Basin.||||||12-JAN-05
15091|Pertaoorrta Group|62376|5|Briefly described|p18|Late Cambrian|Late Proterozoic|Geological Province: Amadeus Basin.||||||09-FEB-10
15091|Pertaoorrta Group|62379|5|Briefly described|p7 Fig. 2|Late Cambrian|Late Proterozoic|Geological Province: Amadeus Basin.||||||
15091|Pertaoorrta Group|62609|5|Briefly described|Map Legend|Cambrian|Cambrian|Sandstone, siltstone, shale, limestone, dolomite, some conglomerate. Marine fossils. Underlies Larapinta Group.||||||14-AUG-06
15091|Pertaoorrta Group|62620|5|Briefly described|Map Legend|Cambrian|Cambrian|Sandstone, siltstone, shale, limestone, dolomite, some conglomerate.||||||
15091|Pertaoorrta Group|62794|5|Briefly described|p289 Fig.2, p290|Late Cambrian|Late Cambrian|Amadeus Basin. Underlies Late Cambrian-Early Ordovician Larapinta Group. Includes Goyder Formation.||||||
15091|Pertaoorrta Group|64334|5|Briefly described|p39-40|Cambrian|Cambrian|Amadeus Basin.||||Is overlain unconformably by Larapinta Group.|Sandstone, limestone, dolostone.|
15091|Pertaoorrta Group|64443|6|Mentioned|p40.|||Of Amadeus Basin. Correlative of Barkly Group, Georgina Basin in part.||||||
15091|Pertaoorrta Group|64778|6|Mentioned|p11, 13|Cambrian|Cambrian|Amadeus Basin. Several thousand meters thick. Appears as Pertaoorta Group on p11.||||||
15091|Pertaoorrta Group|64809|5|Briefly described|p3 Fig.2 |Late Cambrian|Late Proterozoic|Mis-spelt as Pertaoort in Fig.4.|||Includes Mount Currie Cong.; Eninta, Chandler, Tempe, Shannon, Petermann, Goyder Formations; Arumbera, Illara, Cleland Sandstones; Todd River, Giles Creek Dolostones; Hugh River Shale; Jay Creek Lst.|||
15091|Pertaoorrta Group|64970|6|Mentioned|p719 Fig. 2|Cambrian|Neoproterozoic|Geological Province: Amadeus Basin.||||||27-MAY-09
15091|Pertaoorrta Group|65102|6|Mentioned|p363, Figure 4-38|Paleozoic|Neoproterozoic|Amadeus Basin.||||||
15091|Pertaoorrta Group|65233|4|Described|p3 Fig. 2, p7|Early Cambrian|Neoproterozoic|Geological province: Amadeus Basin.||||||07-FEB-11
15091|Pertaoorrta Group|65489|5|Briefly described|p125|Cambrian|Cambrian|Amadeus Basin.|||Includes Todd River Dolomite; Chandler, Giles Creek, Tempe, Shannon and Goyder Formations.|Overlies Arumbera Formation. Is overlain by Larapinta Group.||
15091|Pertaoorrta Group|67326|5|Briefly described|p2|Late Cambrian|Neoproterozoic|Amadeus Basin. Also includes Mount Currie Conglomerate; Todd River, Giles Creek Dolostones. The stratigraphic diagram is not clear: the Group may also include Sir Frederick Conglomerate, Ellis Sandstone, Winnall beds, and Pertatataka and Julie Formations.|||Arumbera, Cleland, Illara, Deception, Petermann Sandstones; Maurice, Eninta, Chandler, Tempe, Shannon, Goyder Formations; Jay Creek Limestone; Hugh River Shale. See Comments for more.|Is overlain by Larapinta Group.||
15091|Pertaoorrta Group|67565|5|Briefly described|p5 Fig.3, p39-41|||Amadeus Basin.|||Includes Arumbera Sandstone, Tempe Formation, Hugh River Shale, Illara Formation, Deception Formation, Petermann sandstone, Cleland Sandstone, Goyder Formation.|||03-DEC-15
15091|Pertaoorrta Group|68323|6|Mentioned|p4 Fig.2|Late Cambrian|Neoproterozoic|Amadeus Basin. Other constituents include Todd River, Giles Creek Dolostones; Hugh River Shale; Jay Creek Limestone.|||Maurice, Eninta, Chandler, Tempe, Shannon, Goyder FZs; Sir Frederick, Mount Currie Conglomerates; Arumbera, Cleland, Illara, Deception, Petermann Sandstones. See Comments for more.|||
15091|Pertaoorrta Group|69438|4|Described|p23:2-4, 23-32, 34, 37, 53|Late Cambrian|Ediacaran|?Ranford et al. (1965). Previously Pertaaoorrta Formation of Wells et al. (1965). Amadeus Basin. Other constituents are Hugh River Shale; Mutitjulu Arkose; Todd River, Giles Creek Dolostones; Jay Creek Limestone; Winnall beds. See also references to mis-spelt Pertaoorta Group (23:4-5, 7-8, 47, 50). Hosts malachite pellets at the Alalgara Cu occurrence.|||Arumbera, Ellis, Eninta, Cleland, Illara, Petermann Sandstones; Namatjira, Chandler, Maurice, Tempe, Deception, Goyder, Shannon Formations; Quandong, Mount Currie Conglomerates; see Comments for more|Is overlain unconformably by Stairway Sandstone (Larapinta Group) and Mereenie Sandstone.||12-JUL-16
15091|Pertaoorrta Group|69443|6|Mentioned|p28:21|||Amadeus Basin.||||Correlated with Barkly Group.||12-JUL-16
15091|Pertaoorrta Group|69449|6|Mentioned|p34:4|Cambrian|Cambrian|Amadeus Basin. Has equivalent rocks in western Warburton Basin in SA, but not yet described from any NT drillholes.||||||12-JUL-16
15091|Pertaoorrta Group|69673|5|Briefly described|p65, p66, p79|Cambrian|Ediacaran||||Includes Arumbera Sandstone,|Unconformably overlain by Stairway Sandstone|Carbonates and siliciclastic rocks.|
15091|Pertaoorrta Group|70749|6|Mentioned|p54|||Amadeus Basin.|||Goyder Formation.|||
15091|Pertaoorrta Group|70752|5|Briefly described|p125|Cambrian|Proterozoic|Amadeus Basin.|||Todd River, Giles Creek Dolostones; Arumbera Sandstone; Shannon, Goyder Formations.|||
15091|Pertaoorrta Group|70839|5|Briefly described|p329|Cambrian|Ediacaran|Of Amadeus Basin. Part of Supersequence 4.|||Includes Arumbera Sandstone.|Underlain by Julie Formation or Arumbera Sandstone.||
15091|Pertaoorrta Group|71088|6|Mentioned|p8, p33|Cambrian|Cambrian|Amadeus Basin.||||Equivalent to the Mu Formation.||
15091|Pertaoorrta Group|71146|5|Briefly described|p6|Cambrian|Cambrian|Amadeus Basin.||||Unconformably overlain by the Pacoota Sandstone (Larapinta Group).|Sandstone, carbonate, mudstone and evaporite.|
15091|Pertaoorrta Group|71268|5|Briefly described|1m_geologyp12_lut.csv||||||Includes Cleland Sandstone.|||
15091|Pertaoorrta Group|71279|5|Briefly described|p355 Fig.2, p382 Tb.1|Late Cambrian|Ediacaran|Amadeus Basin. Other constituents include: Winnall Beds; Todd River, Giles Creek Dolostones; Hugh River Shale; Jay Creek Limestone. Modelled magnetic properties.|||Carnegie, Maurice, Namatjira, Chandler, Deception, Shannon, Goyder Formations; Ellis, Arumbera, Cleland, Illara, Petermann Sandstones; Sir Frederick, Mount Currie Conglomerates. See Comments for more.|||
15091|Pertaoorrta Group|71841|5|Briefly described|p1|Early Cambrian|Ediacaran|Of Amadeus Basin.|||Includes Maurice Formation, Winnall Beds, Sir Frederick Conglomerate, Ellis Sandstone, Mount Currie Conglomerate, Carnegie Formation, Namatjira Formation, Todd Rover Dolostone and Arumbera Sandstone.|Underlain by Boord Formation or Inindia beds or Julie Formation.||
15091|Pertaoorrta Group|71842|5|Briefly described|p3|Early Cambrian|Ediacaran|Of Amadeus Basin.|||Includes Maurice Formation, Sir Frederick Conglomerate, Ellis Sandstone, Mount Currie Conglomerate, Carnegie Formation, Winnall beds, Namatjira Formation, Todd River Dolostone and Arumbera Sandstone.|||
15091|Pertaoorrta Group|71898|4|Described|iii, p1, p6, p8-p9, p11, p14, p17-p18|Late Cambrian|Early Cambrian|Amadeus Basin. Previously the Pertaoorrta Formation of Wells et al, 1965. Outcrops in the AREYONGA (5439) map sheet of HENBURY. Hosts a significant amount of detrital zircons ranging from ca 650-490 Ma.|||Includes the Tempe Formation, Deception Formation, Petermann Sandstone and the Goyder Formation.|Overlain by the Pacoota Sandstone (Larapinta Group).||19-NOV-18
15091|Pertaoorrta Group|72360|5|Briefly described|Solid Geology map|||Of Amadeus Basin.||||||
15091|Pertaoorrta Group|72369|5|Briefly described|p15,20,23,37|Cambrian|Cambrian|Of Amadeus Basin.|||Includes Arumbera and Eninta sandstones.|Underlain by Winnall Group.||
15091|Pertaoorrta Group|72374|5|Briefly described|iii,p3,12,15|Cambrian|Ediacaran|Of Amadeus Basin.|||Includes Eninta Sandstone, Illara Sandstone.|||
15091|Pertaoorrta Group|73085|6|Mentioned|p1|late Cambrian|Ediacaran||||[Unclear]|||
15091|Pertaoorrta Group|73119|6|Mentioned|piii, p14, p16|||Amadeus Basin, western. Dominant detrital zircon age components are Mesoproterozoic, with a major peak between ca 1170 - 1150 Ma and other minor peaks. [See article for provenance discussion].|||Cleland Sandstone, Tempe Formation|||
15094|Pertatataka Formation|9199|5|Briefly described|Map legend|Proterozoic|Proterozoic|Siltstone and shale with lenses of sandstone, limestone, dolomite, conglomerate.  Geological Province: Amadeus Basin.||||||
15094|Pertatataka Formation|9814|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Siltstone, shale.||||||
15094|Pertatataka Formation|22506|6|Mentioned|p130 Fig.4|Neoproterozoic III|Neoproterozoic III|||||||
15094|Pertatataka Formation|22560|5|Briefly described|p2|||||||||
15094|Pertatataka Formation|22561|4|Described|p24|Neoproterozoic|Neoproterozoic|||||||
15094|Pertatataka Formation|22562|6|Mentioned|p39|||||||||
15094|Pertatataka Formation|22564|5|Briefly described|p59||Neoproterozoic|||||||
15094|Pertatataka Formation|22566|5|Briefly described|p73|Neoproterozoic|Neoproterozoic|In the north of the Ooraminna depocentre, the Pertatataka Fromation overlies the lower subunits of the Olympic Formation at this Type Section - p81.||||||
15094|Pertatataka Formation|22567|5|Briefly described|p91|||Age: 730+/-45 Ma Rb-Sr data (Compston and Taylor, 1969).||||||04-SEP-14
15094|Pertatataka Formation|22646|4|Described|p 99|Neoproterozoic|Neoproterozoic|informal name - lower Pertatataka Formation is mentioned on p 101||||||
15094|Pertatataka Formation|22649|5|Briefly described|p 152|Neoproterozoic|Neoproterozoic|Underlain by Gaylad Sandstone.||||||22-NOV-06
15094|Pertatataka Formation|22651|6|Mentioned|Fig 10 btw p182-183|Proterozoic|Proterozoic|||||||
15094|Pertatataka Formation|22652|6|Mentioned|p 222|||||||||
15094|Pertatataka Formation|22653|6|Mentioned|Fig 14 on p 236|||||||||
15094|Pertatataka Formation|22746|5|Briefly described|p513, p529|||||||||
15094|Pertatataka Formation|22761|6|Mentioned|p358|||||||||
15094|Pertatataka Formation|22762|5|Briefly described|p378|Neoproterozoic|Neoproterozoic|||||||
15094|Pertatataka Formation|22763|5|Briefly described|p398|Neoproterozoic|Neoproterozoic|||||||
15094|Pertatataka Formation|22804|6|Mentioned|p440|Neoproterozoic|Neoproterozoic|||||||
15094|Pertatataka Formation|22805|5|Briefly described|p464|Neoproterozoic|Neoproterozoic|||||||
15094|Pertatataka Formation|22816|5|Briefly described|p10 Fig. 4|Neoproterozoic|Neoproterozoic|In the Amadeus Basin.||||||22-NOV-06
15094|Pertatataka Formation|22823|4|Described|p517-518|Proterozoic|Proterozoic|||||||
15094|Pertatataka Formation|22826|4|Described|p570|Neoproterozoic|Neoproterozoic|||||||
15094|Pertatataka Formation|22901|6|Mentioned|78|||Geological  province: Amadeus Basin.||||||22-NOV-06
15094|Pertatataka Formation|22921|6|Mentioned|39|||Geological province: Amadeus Basin.||||||17-APR-13
15094|Pertatataka Formation|23250|5|Briefly described|p1124  Fig.2||Neoproterozoic III|Correlate of Tent Hill Formation and Yarloo Shale, and Bunyeroo Formation, ABC Range Quartzite and Brachina Formation.||||||
15094|Pertatataka Formation|23282|6|Mentioned|p89|||In the Amadeus Basin.||||||22-NOV-06
15094|Pertatataka Formation|23287|6|Mentioned|p104 Fig.4|||Age: Ediacarian. In the Amadeus Basin.||||||22-NOV-06
15094|Pertatataka Formation|23314|5|Briefly described|333 Fig.4|Neoproterozoic III|Neoproterozoic III|||||||
15094|Pertatataka Formation|23356|5|Briefly described|26 Tab.2|Neoproterozoic|Neoproterozoic|Age: ~600Ma.||||||22-NOV-06
15094|Pertatataka Formation|23806|5|Briefly described|p1122 Fig. 1|Neoproterozoic|Neoproterozoic|||||||
15094|Pertatataka Formation|24064|5|Briefly described|p229 Fig.7|Adelaidean|Adelaidean|Geological Province: Amadeus Basin.||||||
15094|Pertatataka Formation|24111|5|Briefly described|p216|Neoproterozoic|Neoproterozoic|Geological Province: Amadeus Basin. See also p215 Fig. 11.||||||
15094|Pertatataka Formation|24301|5|Briefly described|p17|Neoproterozoic|Neoproterozoic|Geological Province: Amadeus Basin||||||
15094|Pertatataka Formation|24442|6|Mentioned|p38|||Geological Province: Centralian Superbasin.||||||
15094|Pertatataka Formation|29721|6|Mentioned|Table 44|||||||||
15094|Pertatataka Formation|29972|6|Mentioned|Table 1|||Proterozoic||||||
15094|Pertatataka Formation|30220|6|Mentioned|p244|||||||||
15094|Pertatataka Formation|30258|6|Mentioned|Fig.2|||About 730m.y.||||||
15094|Pertatataka Formation|30544|6|Mentioned|p48|||On map legend||||||
15094|Pertatataka Formation|31026|6|Mentioned|p61|||||||||
15094|Pertatataka Formation|31566|6|Mentioned|p230|||Proterozoic||||||
15094|Pertatataka Formation|31645|6|Mentioned|Table 2|||Correlation||||||
15094|Pertatataka Formation|32144|6|Mentioned|p81|||Organic matter||||||
15094|Pertatataka Formation|32376|6|Mentioned|p1541|||||||||
15094|Pertatataka Formation|32442|6|Mentioned|p9|||||||||
15094|Pertatataka Formation|32469|6|Mentioned|p531|||||||||
15094|Pertatataka Formation|32720|6|Mentioned|Table 1|||||||||
15094|Pertatataka Formation|32722|6|Mentioned|Fig.3|||Adelaidean. Stromatolite||||||
15094|Pertatataka Formation|33025|6|Mentioned|p928|||Minimum age 800 m.y.||||||
15094|Pertatataka Formation|33102|6|Mentioned|Fig.2|||||||||
15094|Pertatataka Formation|33103|6|Mentioned|p23|||||||||
15094|Pertatataka Formation|33630|6|Mentioned|p906|||||||||
15094|Pertatataka Formation|33655|6|Mentioned|p101|||||||||
15094|Pertatataka Formation|33761|6|Mentioned|p146|||Adelaidean. Contains Olympic Member||||||
15094|Pertatataka Formation|34111|4|Described|Table 1|||Precambrian. See also Table 4, pp11,14,17,19.||||||22-NOV-06
15094|Pertatataka Formation|34186|6|Mentioned|Fig.3|||Late Precambrian. See also Fig.4.||||||
15094|Pertatataka Formation|34202|6|Mentioned|p1058|||||||||
15094|Pertatataka Formation|34287|6|Mentioned|p41|||See also p42.||||||22-NOV-06
15094|Pertatataka Formation|34442|5|Briefly described|Table 1|||Proterozoic||||||
15094|Pertatataka Formation|34488|4|Described|Table 1|||Proterozoic. See also pp10,14,16.||||||22-NOV-06
15094|Pertatataka Formation|34579|5|Briefly described|Table 1|||See also pp15,17, Fig.2.||||||22-NOV-06
15094|Pertatataka Formation|34580|4|Described|Table 1|||||||||
15094|Pertatataka Formation|35064|6|Mentioned|p208|||||||||
15094|Pertatataka Formation|35088|6|Mentioned|p92|||||||||
15094|Pertatataka Formation|35102|6|Mentioned|Fig.2|||||||||
15094|Pertatataka Formation|35136|6|Mentioned|p140|||||||||
15094|Pertatataka Formation|35798|6|Mentioned|p307|||||||||
15094|Pertatataka Formation|35805|5|Briefly described|p36|||See also Fig.3.||||||
15094|Pertatataka Formation|35863|6|Mentioned|Table 1|||||||||
15094|Pertatataka Formation|36198|6|Mentioned|Fig.III.2|||||||||
15094|Pertatataka Formation|36473|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
15094|Pertatataka Formation|36898|6|Mentioned|p198|||||||||
15094|Pertatataka Formation|37371|6|Mentioned|p382|||||||||
15094|Pertatataka Formation|37462|4|Described|Table 4.IX|||||||||
15094|Pertatataka Formation|37572|6|Mentioned|p153|||||||||
15094|Pertatataka Formation|37928|6|Mentioned|p517|||||||||
15094|Pertatataka Formation|37929|6|Mentioned|Fig.2|||||||||
15094|Pertatataka Formation|38157|6|Mentioned|Table VI|||||||||
15094|Pertatataka Formation|38606|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
15094|Pertatataka Formation|38885|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
15094|Pertatataka Formation|38945|6|Mentioned|p134|||||||||
15094|Pertatataka Formation|39210|4|Described|p37|||||||||
15094|Pertatataka Formation|39213|6|Mentioned|Fig.6|||Amadeus Basin Succession||||||
15094|Pertatataka Formation|39558|6|Mentioned|Table 2|||||||||
15094|Pertatataka Formation|39565|6|Mentioned|p32|||||||||
15094|Pertatataka Formation|39583|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
15094|Pertatataka Formation|39898|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Laminated siltstone and shale, sandstone. Geological Province: Amadeus Basin.||||||14-FEB-06
15094|Pertatataka Formation|39931|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
15094|Pertatataka Formation|40105|6|Mentioned|p311|||||||||
15094|Pertatataka Formation|40201|5|Briefly described|Table 1|||||||||
15094|Pertatataka Formation|40740|3|Fully described|p12|||||||||
15094|Pertatataka Formation|40810|6|Mentioned|p3|||||||||
15094|Pertatataka Formation|40852|6|Mentioned|p29|||||||||
15094|Pertatataka Formation|40856|5|Briefly described|p316|||||||||
15094|Pertatataka Formation|41005|6|Mentioned|Fig.2|||||||||
15094|Pertatataka Formation|41039|6|Mentioned|Fig.2|||||||||
15094|Pertatataka Formation|41115|6|Mentioned|p1389|||||||||
15094|Pertatataka Formation|41190|6|Mentioned|Fig.4|||||||||
15094|Pertatataka Formation|41203|6|Mentioned|p5|||||||||
15094|Pertatataka Formation|41224|6|Mentioned|Fig.2|||||||||
15094|Pertatataka Formation|41270|6|Mentioned|Table 1|||||||||
15094|Pertatataka Formation|41429|5|Briefly described|p246|||||||||
15094|Pertatataka Formation|41618|6|Mentioned|Fig.2|||||||||
15094|Pertatataka Formation|41717|5|Briefly described|p355|||||||||
15094|Pertatataka Formation|41801|6|Mentioned|p218|||||||||
15094|Pertatataka Formation|41852|6|Mentioned|p209|||||||||
15094|Pertatataka Formation|42059|6|Mentioned|Fig.2 P131|||||||||
15094|Pertatataka Formation|42060|6|Mentioned|Fig.5 P140|||||||||
15094|Pertatataka Formation|42082|6|Mentioned|Fig.3 P323|||||||||
15094|Pertatataka Formation|42504|5|Briefly described|p72|||||||||
15094|Pertatataka Formation|42643|6|Mentioned|Fig.4 P19|||||||||
15094|Pertatataka Formation|42845|6|Mentioned|Fig.3 P498|||||||||
15094|Pertatataka Formation|42886|4|Described|p223|||see also Fig.2 p219.||||||22-NOV-06
15094|Pertatataka Formation|42940|5|Briefly described|Plate 2|Neoproterozoic|Neoproterozoic|Shale, siltstone.  Geological province: Amadeus Basin.||||||04-SEP-14
15094|Pertatataka Formation|43011|6|Mentioned|Table 2,p12|||||||||
15094|Pertatataka Formation|43057|5|Briefly described|p68|||||||||
15094|Pertatataka Formation|43105|5|Briefly described|Fig.3,p8|||||||||
15094|Pertatataka Formation|43225|5|Briefly described|Map Legend||Neoproterozoic|||||||
15094|Pertatataka Formation|43503|6|Mentioned|11-50|||from Ediacaran to||||||
15094|Pertatataka Formation|43595|5|Briefly described|p548,Fig.5-33,549||Adelaidean|||||||
15094|Pertatataka Formation|43622|6|Mentioned|p39|||||||||
15094|Pertatataka Formation|43647|6|Mentioned|Fig.4,533|||||||||
15094|Pertatataka Formation|43648|6|Mentioned|p491|||||||||
15094|Pertatataka Formation|43649|5|Briefly described|p457|||||||||
15094|Pertatataka Formation|43756|6|Mentioned|p542|||||||||
15094|Pertatataka Formation|43817|6|Mentioned|Fig.1,p42|||||||||
15094|Pertatataka Formation|44261|14|Not recorded|p7-19|||Not recorded on white card.||||||
15094|Pertatataka Formation|44262|14|Not recorded|p3-21|||Not listed on white card.||||||
15094|Pertatataka Formation|44335|4|Described|p.7||Proterozoic|Tb.1. p.8.||||||
15094|Pertatataka Formation|44342|14|Not recorded|p.5|||SG/53-5, correlated with Winnall Beds.||||||
15094|Pertatataka Formation|44395|14|Not recorded|p.6|||Correlates with Ellis Sandstone and Maurice Formation.||||||22-NOV-06
15094|Pertatataka Formation|44402|5|Briefly described|map legend||Proterozoic|||||||02-DEC-04
15094|Pertatataka Formation|44433|14|Not recorded|map legend||Proterozoic|||||||
15094|Pertatataka Formation|44484|14|Not recorded|p.10, Fig.4, Tb.1||Proterozoic|||||||
15094|Pertatataka Formation|44485|14|Not recorded|map legend||Proterozoic|||||||
15094|Pertatataka Formation|44497|4|Described|p.6, Table 1||Proterozoic|SF/53-13.||||||
15094|Pertatataka Formation|44498|14|Not recorded|map legend||Proterozoic|||||||
15094|Pertatataka Formation|44505|14|Not recorded|p.7, Fig.1, Table 1||Proterozoic|||||||
15094|Pertatataka Formation|44506|14|Not recorded|map legend||Proterozoic|||||||
15094|Pertatataka Formation|45041|4|Described|p32|||Proterozoic||||||
15094|Pertatataka Formation|45052|6|Mentioned|p67|||||||||
15094|Pertatataka Formation|45079|6|Mentioned|p16|||||||||
15094|Pertatataka Formation|46730|5|Briefly described|p7|||Underlain by Pioneer Sandstone. Geological Province: Amadeus Basin||||||22-NOV-06
15094|Pertatataka Formation|46829|6|Mentioned|Fig.2|||||||||
15094|Pertatataka Formation|46865|4|Described|p51|||||||||
15094|Pertatataka Formation|46903|6|Mentioned|Fig.3|||Magnetic polarity sequences||||||
15094|Pertatataka Formation|46928|6|Mentioned|Table 1|||||||||
15094|Pertatataka Formation|47035|6|Mentioned|Fig.1|||||||||
15094|Pertatataka Formation|48639|14|Not recorded|p.13,opp.p.1||Neoproterozoic|See also page, 11. Pl.2,Sh.2. U.Prot. (G55-2,15,G53-3).||||||
15094|Pertatataka Formation|48838|2|Defined|p.13, Tb.1|||||||||
15094|Pertatataka Formation|48844|14|Not recorded|p.8|||||||||
15094|Pertatataka Formation|48862|14|Not recorded|p.8|||On many pages. p.1,8,13,16,18,21,34,38,41,43; opp.8,9; Pl.2,7,10. (F52-15).||||||
15094|Pertatataka Formation|48863|2|Defined|p.12|||Tb.1. opp.p.7,9,11,17,38-40, Pl.15,16. ?Upper Proterozoic, or Lower Cambrian. (G52-4,G53-1).||||||
15094|Pertatataka Formation|48864|14|Not recorded|Tb.1,p.1,26,31|||||||||
15094|Pertatataka Formation|48865|14|Not recorded|Fig.4,p.20,45|||(F53-13).||||||
15094|Pertatataka Formation|48880|14|Not recorded|p.20,20,33,Pl.10-13||Neoproterozoic|U.Prot. 750 m.y. (F53-13,14).||||||
15094|Pertatataka Formation|48890|4|Described|p.22-31|||See also Tables, Figs and Plates. Includes: Ringwood Member, Olympic Member, Limbla Member, Julie Member, Cyclops Member. Defn on Tech.File F/53-13.||||||22-NOV-06
15094|Pertatataka Formation|48963|6|Mentioned|p5|||||||||
15094|Pertatataka Formation|48990|6|Mentioned|p11|||||||||
15094|Pertatataka Formation|49796|5|Briefly described|Sect C BDF 28|||||||||
15094|Pertatataka Formation|50246|5|Briefly described|p20 Fig. 2|Proterozoic|Proterozoic|Includes the Cyclops Member.||||||07-FEB-11
15094|Pertatataka Formation|60547|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Siltstone and shale with lenses of sandstone, limestone, dolomite, conglomerate. Geological Province: Amadeus Basin.||||||07-JUN-05
15094|Pertatataka Formation|60549|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Contains the Waldo Pedlar Member.  Laminated siltstone and shale, some sandstone.||||||02-FEB-05
15094|Pertatataka Formation|60674|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|White to yellow-brown, laminated and thinly-bedded fine kaolinitic sandstone with interbeds of laminated micaceous siltstone.  Geological Province: Amadeus Basin.||||||
15094|Pertatataka Formation|61385|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Siltstone, shale, sandstone; limestone with stromatolites. Geological Province: Amadeus Basin.||||||
15094|Pertatataka Formation|61387|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Laminated and thin-bedded, fine kaolinitic sandstone, with interbeds of micaceous siltstone. Geological Province: Amadeus Basin.||||||04-OCT-05
15094|Pertatataka Formation|61518|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Laminated and thin bedded fine grained kaolinitic sandstone with interbeds of micaceous siltstone. Geological Province: Amadeus Basin.||||||
15094|Pertatataka Formation|61519|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Laminated and thin bedded, fine kaolinitic sandstone with interbeds of micaceous siltstone. Geological Province: Amadeus Basin.||||||
15094|Pertatataka Formation|61732|3|Fully described|p4 Fig. 3, p94-95|Marinoan|Marinoan|Formerly incl. six members: Limbla and Ringwood Members and Olympic and Julie "Members" all now redefined; but retains Cyclops and Waldo Pedlar Members. Max. thickness: 570m. Geol.Prov: Amadeus Basin. See also p5 Tb. 1.||||||10-SEP-14
15094|Pertatataka Formation|62085|6|Mentioned|p15 Fig.1, p20  |||Amadeus Basin. Contains distinctive acritarch assembly: Appendisphaera barbata.|||||Marine siltstone.|
15094|Pertatataka Formation|62376|5|Briefly described|p18|Late Proterozoic|Late Proterozoic|Geological Province: Amadeus Basin.||||||09-FEB-10
15094|Pertatataka Formation|62379|5|Briefly described|p7 Fig. 2, p26|Late Proterozoic|Late Proterozoic|Geological Province: Amadeus Basin. Thickness: 600m. Black shale. Lateral equivalent of Winnall beds.||||||
15094|Pertatataka Formation|62428|5|Briefly described|p351 Tb. 6|Early Cambrian|Neoproterozoic III|Palaeomagnetic data.||||||10-FEB-09
15094|Pertatataka Formation|62453|5|Briefly described|p12 Fig. 8|Ediacaran|Ediacaran|Geological Province: Amadeus Basin.||||||
15094|Pertatataka Formation|62595|5|Briefly described|p29 Fig.6.|Proterozoic|Proterozoic|Ross River area.|||Includes Cyclops Member.||Sandstone, fine-grained, undulose to flat and laminated and fissile.|
15094|Pertatataka Formation|62620|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Siltstone, shale, limestone, calcarenite, dolomite, some sandstone and tillitic conglomerate.||||||
15094|Pertatataka Formation|62903|6|Mentioned|p730 Fig.1|||Amadeus Basin. Presented in figure as Pertatataka, and Pertatataka Fm.||||overlies Cap Dolomite; is overlain by Julie Formation.||
15094|Pertatataka Formation|63458|6|Mentioned|p897 Fig.19. |Ediacaran|Ediacaran|Amadeus Basin.||||Is overlain by Julie Formation.||
15094|Pertatataka Formation|63562|5|Briefly described|p338 fig 3, p343, 344, p352 fig 10|Ediacaran|Ediacaran|Of Amadeus Basin. Coarsens to the S, implying source in Musgrave Inlier.||||Overlies Pioneer Sandstone.|Deep-water turbidites and pelagic sediments.|
15094|Pertatataka Formation|63811|6|Mentioned|p503,505, p519-527 App A|Ediacaran|Ediacaran|Of Amadeus Basin. Has acritarch fossils in common with Ungoolya Group, Officer Basin, and Doushantuo Formation, South China. Also correlated with Khamaka and Kursov Formations, Siberia.||||||28-MAR-12
15094|Pertatataka Formation|64068|6|Mentioned|p49, 51, 224|||Amadeus Basin. Lower part correlated with Gnallan-a-Gea Arkose, Elyuah Formation, medial to upper part with Grant Bluff Formation, southern Georgina Basin.||||||
15094|Pertatataka Formation|64625|5|Briefly described|p243-257|Neoproterozoic|Neoproterozoic|Amadeus Basin. Has a basal "cap carbonate".|||Includes Cyclops Member|Overlies Gaylad Sandstone, Pioneer Sandstone. Is overlain gradationally by Julie Formation.|Siltstone and shale, sandstone.|
15094|Pertatataka Formation|64724|5|Briefly described|p49 Fig. 7|Ediacaran|Ediacaran|Deposited in the Amadeus Basin during the Centralian 3 event (~600-544 Ma)||||||
15094|Pertatataka Formation|64778|6|Mentioned|p13, 18|Neoproterozoic|Neoproterozoic|Amadeus Basin.||||||
15094|Pertatataka Formation|64794|6|Mentioned|p238 fig 2|Ediacaran|Ediacaran|||||||
15094|Pertatataka Formation|64797|5|Briefly described|p152, p153 Fig.2, p157-159 |||See also p164 Fig.11, p167 Tb.10, p168 Tb.11, p176-177. Of Amadeus Basin. S-isotope data.||||Correlated with Brachina Formation (Adelaide Rift Complex).||
15094|Pertatataka Formation|64809|5|Briefly described|p2, p3 Fig.2, p6 Fig.4, p11 Fig.10.|Proterozoic|Proterozoic|See also p13 Fig.13, p15 Fig.15. Widespread transgressive deposits.|||Includes Cyclops Member.||Fine marine siliciclastics (siltstone, shale).|
15094|Pertatataka Formation|64970|6|Mentioned|p719 Fig. 2|Neproterozoic|Neoproterozoic|Geological Province: Amadeus Basin.||||||27-MAY-09
15094|Pertatataka Formation|65233|3|Fully described|p3 Fig. 2, p6|Neoproterozoic|Neoproterozoic|Formerly Winnall beds. Disconformable on Bitter Springs Fm; disconform.or conform.on Olympic Fm; below Julie Fm. Max.thick: 500m. Amadeus Basin.Thick extensive marine shales in succession of mainly fine-gr.clastics, predom'l red/green shale+ fine-gr. sst||||||07-FEB-11
15094|Pertatataka Formation|65256|6|Mentioned|p19|||Stratigraphic correlative of the Winnall beds.||||||
15094|Pertatataka Formation|65272|6|Mentioned|p320 Fig.3||Ediacaran|||||||
15094|Pertatataka Formation|65338|5|Briefly described|p64.|||Amadeus Basin. Correlative with Elyuah Formation.|||||Predominantly micaceous siltstone and shale with thinly interbedded sandstone; rare limestone.|
15094|Pertatataka Formation|65342|5|Briefly described|p4.|||Amadeus Basin. Max. thickness at least 19 m.||||Is overlain by Julie Formation.|Fine kaolinitic sandstone.|
15094|Pertatataka Formation|65365|5|Briefly described|p10 Fig. 4|Ediacaran|Ediacaran|Amadeus Basin. Includes Acanthomorph acritarchs.||||||
15094|Pertatataka Formation|65366|5|Briefly described|p23 Fig. 3|Ediacaran|Ediacaran|Amadeus Basin||||||
15094|Pertatataka Formation|65410|6|Mentioned|p74.|Neoproterozoic|Neoproterozoic|Amadeus Basin. Part of Supersequence 3. Contains distinctive, well-documented and well-constrained palynomorph assemblages of biostratigraphic significance, including acritarchs.||||||
15094|Pertatataka Formation|65416|6|Mentioned|p141, p146.|||Amadeus Basin. Tentatively correlated with Boondawari Formation (Officer Basin). Suggested by Perincek (1996) to pre-date the Petermann Ranges Orogeny.||||||
15094|Pertatataka Formation|65489|5|Briefly described|p125|Proterozoic|Proterozoic|Amadeus Basin.||||Overlies Aralka Formation. Is overlain by Arumbera Formation.||
15094|Pertatataka Formation|65892|6|Mentioned|p35.|Late Neoproterozoic|Late Neoproterozoic|Amadeus Basin. Contains same acritarchs as Bunyeroo and lower Wonoka Formations, Adelaide Geosyncline.||||||
15094|Pertatataka Formation|66767|5|Briefly described|p60|Neoproterozoic|Neoproterozoic|NE Amadeus Basin. 350m thick in its type section; locally up to 1400m thick. Deep-water, pelagic deposits.|||||Predominantly red and green siltstone, shale and feldspathic sandstone.|
15094|Pertatataka Formation|67326|4|Described|p2, p7-10, Appx.2|Neoproterozoic|Neoproterozoic|Amadeus Basin. Intersected by stratigraphic drillhole BRD05DD01. Over 450m thick. South of the Angas Lineament Zone (previously the Central Ridge), the Winnall beds are widespread and 400-500m thick; the authors state that the term is redundant, and the rocks subsumed into the Pertatataka Formation. Probable source of gas in the Dingo gas field; a potential source rock for dry gas over wide areas of the Basin. Rockeval Pyrolysis results discussed. Core section photographs. Composite log.||||Conformably to disconformably overlies Olympic or Bitter Springs Formations. Is overlain by Julie Formation.|Red-brown to occasionally grey siltstone and mudstone, becoming evaporitic towards the top. Occasional upward-fining cycles representing turbidity current deposits.|
15094|Pertatataka Formation|67484|6|Mentioned|p294 Tb.1|Ediacaran|Ediacaran|Amadeus Basin.||||Overlain by the Julie Formation. Underlain by the Olympic Formation.||
15094|Pertatataka Formation|67565|5|Briefly described|p5 Fig.3, p39, p46.|Ediacaran|Ediacaran|Amadeus Basin. Deep water siliciclastic sediments. Forms strike ridges. 350 m thick, increasing to the west.||||Is overlain unconformably by the Arumbera Sandstone.|White to yellow-brown, laminated and thinly-bedded, fine-grained kaolinitic sandstone; poorly exposed interbeds of laminated micaceous siltstone.|
15094|Pertatataka Formation|67620|6|Mentioned|p5, 22|Ediacaran|Ediacaran|Amadeus Basin. Contains abundant organic laminae (microbial mats).||||Overlies Olympic Formation. Is overlain by Julie Formation.||
15094|Pertatataka Formation|67856|5|Briefly described|p338 fig 4-30, p337, p345 |Neoproterozoic|Neoproterozoic|||||Underlain by Olympic Formation.||
15094|Pertatataka Formation|67912|6|Mentioned|p12, 25-27|||Amadeus Basin. Contains diverse assemblages of complex, large acritarchs.||||||
15094|Pertatataka Formation|68270|5|Briefly described|p679,683-684|Ediacaran|Ediacaran|Amadeus Basin.||||Overlain by Julie Formation. Underlain by Pioneer Sandstone and Olympic Formation.||
15094|Pertatataka Formation|68271|6|Mentioned|p696|||Adelaide Rift Complex.||||||
15094|Pertatataka Formation|68275|6|Mentioned|p61|||Variations in the Ediacaran sulfur-isotope record world-wide are briefly discussed.||||||
15094|Pertatataka Formation|68276|6|Mentioned|p71, 73-74|||Amadeus Basin. The ""Formation"" is omitted.",,||||Conformably overlies Olympic Formation.|Reddish-grey laminated siltstone with limestone turbidites.|
15094|Pertatataka Formation|68323|6|Mentioned|p4 Fig.2|Neoproterozoic|Neoproterozoic|Amadeus Basin.||||||
15094|Pertatataka Formation|68473|6|Mentioned|p531|||Amadeus Basin.||||||
15094|Pertatataka Formation|68733|6|Mentioned|p189 Fig.8|Ediacaran|Ediacaran|Amadeus Basin.||||||
15094|Pertatataka Formation|69031|6|Mentioned|p4, p9|||Amadeus Basin. Formerly part of Boord Formation (name discontinued).||||||
15094|Pertatataka Formation|69437|5|Briefly described|p22:4-5, 7|Ediacaran|Ediacaran|NE Amadeus Basin, Centralian A Superbasin. Supersequence 3.||||Overlies Pioneer and Gaylad Sandstones. Is overlain by Julie Formation.|Siltstone and shale.|12-JUL-16
15094|Pertatataka Formation|69438|2|Defined|p23:2-5, 7-8, 10, 17-21, 27,43,47, 59-60|Ediacaran|Ediacaran|Pritchard and Quinlan (1962). The type section is 5km W of Ellery Creek and c.350m thick. Originally defined with two clastic units separated by a dolomite layer. Only the lower clastic unit remains to constitute the Formation; the other units are now the Olympic and Julie Formations. Amadeus Basin. Up to 1400m thick. Generally recessive; the Cyclops Member forms low ridges in places. Previously correlated with Winnall beds, but that unit is now correlated with Carnegie Formation and Arumbera Sandstone. One of the most likely oil- and/or gas-prone units in the Basin. Thick shales form seals over older reservoirs.|||Cyclops, Waldo Pedlar Members.|Disconformably overlies Olympic Formation, Pioneer Sandstone or Bitter Springs Formation. Is overlain conformably by Julie Formation.|Mainly (320m) red and green siltstone and shale, with flaser bedding, small-scale cross-laminations and thin interbeds of fine-grained sandstone; overlain by 1.5m of grey medium-grained feldspathic silicified sandstone and 30m of red siltstone.|12-JUL-16
15094|Pertatataka Formation|69443|6|Mentioned|p28:10|||Amadeus Basin. Correlates with part of the Mopunga Group (Georgina Basin).||||||12-JUL-16
15094|Pertatataka Formation|69606|4|Described|p1, p4 fig 2, p5, p6 fig 3, p7 fig 4, |Early Ediacaran|Early Ediacaran|c. 300m thick. Potential source and seal rock. Amadeus Basin. Type area In north-central Amadeus Basin mentioned. Contact with the Julie Formation is poorly exposed. See also  p14, p15 fig 8, p16, p18, p19.||||Overlies the Pioneer Sandstone and the Olympic Formation. Conformably (gradational) overlain by the Julie Formation.|Red and green siltstone, shale and minor sandstone.|
15094|Pertatataka Formation|69673|5|Briefly described|p63, p74, p80, p81, p86, p88, p90, p97,|Neoproterozoic|Neoproterozoic|Up to 1400m thick. Potential source rock and unconventional gas potential.|||Includes Cyclops Member, Waldo Pedlar Member|Overlain by Julie Formation, conformably overlies Gaylad Sandstone, overlies Pioneer Sandstone, correlated with Winnall beds|Siltstone, shale and feldspathic sandstone.|
15094|Pertatataka Formation|69937|5|Briefly described|v Fig.1, vi, p3 Tb.1, p14, p20, p23|Neoproterozoic|Neoproterozoic|See also p25-31, p51-54. Amadeus Basin. Inferred depositional age of ~575 Ma.|||Cyclops, Waldo Pedlar Members.|Overlies Olympic Formation unconformably and Gaylad Sandstone conformably. Is overlain conformably by Julie Formation.|Mainly grey-green and purple-brown laminated, micaceous siltstone and shale with thin interbeds of sandstone and limestone.|
15094|Pertatataka Formation|70018|5|Briefly described|p235|Neoproterozoic|Neoproterozoic|Amadeus Basin. Of Supersequence 3 in the northern Amadeus Basin. Correlable to Inindia Beds in the southern Amadeus Basin.||||Overlain by Julie Formation. Underlain by Pioneer Sandstone.||
15094|Pertatataka Formation|70416|5|Briefly described|p63-65, p80|Ediacaran|Ediacaran|Amadeus Basin. Earlier definitions included rocks subsequently assigned to Aralka Formation.|||Waldo Pedlar, Cyclops Members.|Overlies Olympic Formation and Pioneer Sandstone. Is overlain by Julie Formation.||
15094|Pertatataka Formation|70839|5|Briefly described|p329|Ediacaran|Ediacaran|Of Amadeus Basin.|||Includes Gaylad Sandstone.|Overlain by Julie Formation. Underlain by Olympic Formation or Pioneer Sandstone.||
15094|Pertatataka Formation|71001|5|Briefly described|p18 Fig.2, p20, 23, 27-28|Ediacaran|Ediacaran|Amadeus Basin. Marine deposits. Carbon isotope correlation graph.|||Waldo Pedlar, Cyclops Members.|Overlies Gaylad Sandstone. Is overlain by Julie Formation.|Dominantly marine pyritic shale.|
15094|Pertatataka Formation|71080|6|Mentioned|p29 fig 20, p30, 31|Ediacaran|Ediacaran|Amadeus Basin. Supersequence 3. Probable source rock for Dingo Field in eastern Amadeus.|||||Dominantly shale in WA. Includes carbonate and sandstone in NT.|
15094|Pertatataka Formation|71088|5|Briefly described|p2, p8, p15|lower Ediacaran|lower Ediacaran|Northern and eastern Amadeus Basin. The lower part of this formation was correlated with the Ellis Sandstone, Sir Frederick Conglomerate and the Maurice Formation by Wells et al., 1970; Grey, 1990; Lindsay and Korsch, 1991.||||||
15094|Pertatataka Formation|71279|5|Briefly described|p353, p355 Fig.2, p365-368, p370, p382|Ediacaran|Ediacaran|Amadeus Basin. Contains interbedded reduced and oxidised iron-rich layers. Contains zircons aged c.1.3 to 0.8 Ga sourced from Tjauwata Group (Musgrave Province). Magnetisation discussed in detail. Modelled magnetic properties.|||||Highly weathered grey-green shale and salty dolomite.|
15094|Pertatataka Formation|71288|6|Mentioned|p146|||Implications of a c.540 Ma paleopole position from this unit discussed.||||||
15094|Pertatataka Formation|71344|4|Described|p1092, 1094, 1095, 1096-1103|Ediacaran||Amadeus Basin. Includes acritarch assemblages that give depositional age constraints (Zhou et al., 2007). Deposited under marine conditions. 300-550 m thick.|635 - 582 Ma|Of Pertaoorta Package.|Includes Waldo Pedlar Member, Cyclops Member.|Conformably overlies the Olympic Formation, Gaylad Sandstone and is succeeded by the Julie Formation.|Red, green to dark green shales and siltstones. Lower and middle part dominated by laminated, dark grey, pyritic siltstone and shale.|10-NOV-17
15094|Pertatataka Formation|71800|6|Mentioned|p26 fig 3|Ediacaran|Ediacaran|Amadeus Basin.||||Overlain by the Julie Formation.||
15094|Pertatataka Formation|71801|6|Mentioned|p230-p231|Ediacaran|Ediacaran|Amadeus Basin.||||Overlain by the Julie Formation.||
15094|Pertatataka Formation|71810|5|Briefly described|Map legend.|Ediacaran|Cryogenian|Amadeus Basin (Phase 1), Centralian Superbasin.|||||Siltstone, shale, and minor sandstone; very poorly exposed.|
15094|Pertatataka Formation|71841|5|Briefly described|p1-2,13|Ediacaran|Ediacaran|Of Amadeus Basin. Original stratigraphy based on McKinnon-Matthews (2009): CPD003: 181.3-219m EOH. Revised stratigraphy in drill core: not intersected.|||Includes Cyclops and Waldo Pedlar members.|Overlain by Julie Formation. Underlain by Pioneer Sandstone or Gaylad Sandstone. Grades into Inindia beds.||
15094|Pertatataka Formation|71842|5|Briefly described|p1-3,9|Ediacaran|Ediacaran|Of Amadeus Basin. Nomenclature after Edgoose 2013 (NE Amedeus, NT).|||Includes Cyclops Member and Waldo Pedlar Member.|Overlain by Julie Formation. Underlain unconformably by Olympic/Pioneer Formation. Correlable with Winnall beds.||
15094|Pertatataka Formation|71898|5|Briefly described|p6|||Amadeus Basin.||||Unconformably (possibly) overlain by the Quandong Conglomerate.||
15094|Pertatataka Formation|72360|5|Briefly described|Solid Geology map|||Of Amadeus Basin.||||||
15094|Pertatataka Formation|72369|4|Described|iii,p3-4,11,14-p15|||Of Amadeus Basin. Originally of Pritchard and Quinlan, 1962. Maidment (2005) provided an inferred depositional age of 575 Ma; further inferred age constraint provided by its stratigraphic position above the Gaylad Sandstone that was deposited during the c. 640-580 Ma Elatina Glaciation (Walter et al 1995). LA-ICP-MS U-Pb detrital zircon dating of sample HB15ND364 (very coarse- to coarse grained sandstone) yielded an interpreted maximum depositional age of 822+\-11 Ma (youngest concordant zircon) does not further constrained the depositional age of the Pertatataka Formation as it is significantly older than the 575 Ma inferred depositional age of Maidment (2005). Contains significant proportion of detrital zircons derived from Musgrave Province (between c. 1500 Ma and c. 970 Ma age spectrum), and Aileron and Warumpi provinces (c. 1810 to c. 1625 Ma age spectrum), and minor Archean-Plaeoproterozoic (>c. 1780 Ma) and Neoproterozoic zircons indicate potential distal sources from the Amadeus Basin. Sample locality, zircon description, SHRIMP results and analyses are discussed.|||Includes Waldo Pedlar and Cyclops members.|Overlain by Winnall Group. Overlies the Gaylad Sandstone.|Red and green siltstone, shale, and fine to medium-grained feldspathic sandstone. Fine to medium-grained, red-brown quartz sandstone.|18-DEC-19
15094|Pertatataka Formation|72374|5|Briefly described|p14|||Of Amadeus Basin. Provenance spectra of Waldo Pedlar Member dominated by Musgrave Province-sourced zircon with lesser zircon sourced from Aileron and Warumpi provinces.|||Includes Waldo Pedlar Member.|||11-OCT-19
15094|Pertatataka Formation|72375|4|Described|p1-2,19-20,23,25,27,29,31|Neoproterozoic|Neoproterozoic|Of Amadeus Basin. Nomenclature of Pritchard and Quinlan 1962. Intepreted maximum depositional age of c. 575 Ma (Maidment 2005). Deep water depositional environment.|||Includes Waldo Pedlar Member, Cyclops Member.|Overlain conformably by Julie Formation. Underlain unconformably by Gaylad Sandstone.|Grey-green and purple-brown laminated, micaceous siltstone and shale with thin interbeds of sandstone and limestone.|
15094|Pertatataka Formation|72489|6|Mentioned|p4 Fig.3, p4|Ediacaran|Ediacaran|Located in the Amadeus Basin.|>548.8 +/- 1 Ma|||Overlain by Julie Formation.||
15094|Pertatataka Formation|72516|6|Mentioned|p88-89|Ediacaran|Ediacaran|Amadeus Basin.|||Includes the Cyclops Member.|Lower part equivalent to the Elyuah Formation. Cyclops Member equivalent to Grant Bluff Formation.||02-JUN-21
15094|Pertatataka Formation|72601|5|Briefly described|p3-4, p7-9, p11-12, p17, p25|Ediacaran|Ediacaran|Amadeus Basin. Preiss et al. (1978) subdivided the original Pertatataka Formation into five formations; Aralka Formation, Olympic Formation (former Olympic Member), Pioneer Sandstone, the revised Pertatataka Formation, and Julie Formation.||||Underlain by Olympic Formation and Pioneer Sandstone. Overlain by Julie Formation.||
15094|Pertatataka Formation|73085|4|Described|piii, p1, p3, p15-16, p18-19, p26-27|Ediacaran|Ediacaran|Amadeus Basin. Lithology is here described from a 136-metre-thick equivalent in drillhole BR05DD01. Sharp contact with underlying Aralka Formation marked by abrupt lithological change.|||Cyclops Member, Waldo Pedlar Member|Unconformably underlain by Aralka Formation, Pioneer Sandstone [/ Olympic Formation] and Gaylad Sandstone. Overlain by Julie Formation. Equivalent to Inindia beds.|Red-brown calcareous siltstone and fine-grained sandstone, micaceous, becoming green-grey siltstone with fine-grained sandstone intervals, calcareous.|
15094|Pertatataka Formation|73086|1|Redefined|[See comments].|Ediacaran|Ediacaran|[Defined herein. No revised definition card]. Post-glacial transgressive unit. Characterised by red and green siltstone with localised conglomerate. Amadeus Basin. Part of Supersequence III. Named was first used by Madigan (1932) from a dictionary of the Arunta language meaning red rock. Type section: Ellery Creek. Key locality: Olympic Bore. Distribution: extends across most of the eastern and central parts of the basin although it is generally poorly exposed (typically only several metres thick); exposures are best in the northeast. Type section thickness: 350 m. Maximum thickness: 1800 m. Originally included several units that were later separately defined such as Ringwood Member, Limbla Member, Aralka Formation, Olympic Formation, Julie Formation. Undivided Pertatataka Formation siltstones referred to as lower, middle or upper Pertatataka Formation according to position relative to formal members, or as undivided Pertatataka Formation where specific level is uncertain or referring to the unit as a whole. Can be difficult to distinguish the unit from siltstones of the Aralka Formation and non-diamictite lithologies of the Olympic Formation. No known macrofossils; large sphaeromorph and acanthomorph acritarch assemblages found in this unit; used to correlate with Rodda beds. Inferred depositional age of 575 Ma (Maidment, 2005). A detrital zircon maximum depositional age of ca 807 Ma is significantly older than the inferred true depositional age. Thinly bedded siltstone represents a quiet, marine depositional setting. Also correlates to Rodda beds, Elyuah Formation, Grant Bluff Formation, Gnallan-a-gea Arkose, Cox Formation, Bukalara Formation, Buckingham Bay Sandstone, Raiwalla Shale, Mount Doreen Formation, Bunyeroo Formation, Brachina Formation, ABC Range Quartzite. p: 3, 5-6, 53, 71-72, 75, 78-79, 90-91, 99-101, 107, ~113-118, 121-135, 143, 160, 163-169, 171.|ca 570 Ma||Cyclops Member, Waldo Pedlar Member|Conformably underlain by Pioneer Sandstone, Olympic Formation, Gaylad [Sandstone]. Overlain by Julie Formation. Correlates to upper Inindia beds and more [see comments].|Red and green siltstone with lenticular bedding, small-scale cross-laminations, and thin interbeds of sandstone overlain by grey, medium-grained, silicified, feldspathic sandstone, which in turn is overlain by red siltstone with sandstone laminae.|
15094|Pertatataka Formation|73088|6|Mentioned|p1|Ediacaran|Ediacaran|Amadeus Basin, northeast.|||Cyclops Member, Waldo Pedlar Member|Unconformably underlain by Pioneer Sandstone and Gaylad Sandstone. Overlain by Julie Formation.||
15094|Pertatataka Formation|73180|4|Described|p47-49, p51 Fig.6, p52|Neoproterozoic|Neoproterozoic|Amadeus Basin.|||Cyclops Member and Waldo Pedlar Members|Conformably overlies the Olympic Formation and Pioneer Sandstone, conformably underlies the Julie Formation.|Primarily red, brown and green shales, siltstones and fine sandstones.|
15094|Pertatataka Formation|73279|5|Briefly described|p3, p6-7|Ediacaran|Ediacaran|Amadeus Basin, eastern. Detrital zircons analysed for Hf isotopic composition [see article].||||May be equivalent to Gloaming Formation.|Includes sandstone.|
15099|Pertnjara Group|9199|5|Briefly described|Map legend|Devonian|Devonian|Includes the Brewer Conglomerate and Hermannsburg Sandstone.  Geological Province: Amadeus Basin.||||||04-NOV-04
15099|Pertnjara Group|9814|5|Briefly described|Map Legend|Devonian|Devonian|||||||
15099|Pertnjara Group|22560|5|Briefly described|p3|Late Devonian|Middle Devonian|||||||
15099|Pertnjara Group|22561|4|Described|p26||Early Devonian|||||||
15099|Pertnjara Group|22564|4|Described|p60||Devonian|Min age - ? Carboniferous.  Underlain by Mereenie Sandstone.||||||22-NOV-06
15099|Pertnjara Group|22566|5|Briefly described|p84|Carboniferous|Early Devonian|||||||12-APR-12
15099|Pertnjara Group|22646|6|Mentioned|p 105|||||||||
15099|Pertnjara Group|22650|5|Briefly described|p 165|Carboniferous|Devonian|||||||
15099|Pertnjara Group|22651|6|Mentioned|Fig 10 btw p182-183||Devonian|||||||
15099|Pertnjara Group|22655|5|Briefly described|p 255|||||||||
15099|Pertnjara Group|22656|6|Mentioned|p 277||Devonian|||||||
15099|Pertnjara Group|22657|6|Mentioned|p 297|Devonian|Devonian|||||||
15099|Pertnjara Group|22760|4|Described|p333-337|Late Devonian|Middle Devonian|||||||
15099|Pertnjara Group|22761|6|Mentioned|p350|Late Devonian|Early Devonian|||||||
15099|Pertnjara Group|22762|5|Briefly described|p377||Devonian|Distal equivalent to the Finke Group p376.||||||
15099|Pertnjara Group|22763|6|Mentioned|p394||Late Devonian|||||||
15099|Pertnjara Group|22804|4|Described|p442|Carboniferous|Middle Devonian|||||||
15099|Pertnjara Group|22805|5|Briefly described|p465||Middle Devonian|||||||
15099|Pertnjara Group|22807|6|Mentioned|Fig 3 on p495|||Age - (?)Middle Devonian-(?)Late Devonian.||||||
15099|Pertnjara Group|22824|5|Briefly described|p525|||||||||
15099|Pertnjara Group|23282|6|Mentioned|p83|||May correlate with Mimili Formation. In the Amadeus Basin.||||||22-NOV-06
15099|Pertnjara Group|23361|5|Briefly described|15|Devonian|Devonian|||||||
15099|Pertnjara Group|23732|5|Briefly described|p31|Late Devonian|Devonian|Geological Province: Amadeus Basin.||||||
15099|Pertnjara Group|23858|5|Briefly described|p913|Devonian||Underlain by Mereenie Sandstone. Geological Province: Amadeus Basin.||||||22-NOV-06
15099|Pertnjara Group|24063|5|Briefly described|p220|Early Carboniferous|Late Devonian|Geological Province: Amadeus Basin. Maximum thicknes: 3650m.||||||
15099|Pertnjara Group|24064|5|Briefly described|p229 Fig.7|Carboniferous|Devonian|Geological Province: Amadeus Basin.||||||
15099|Pertnjara Group|24111|6|Mentioned|p214 Fig. 9|||Geological Province: Amadeus Basin.||||||
15099|Pertnjara Group|29442|6|Mentioned|p103|||||||||
15099|Pertnjara Group|29721|6|Mentioned|Table 44|||||||||
15099|Pertnjara Group|29807|6|Mentioned|p13|||||||||
15099|Pertnjara Group|29817|6|Mentioned|p13|||||||||
15099|Pertnjara Group|29972|6|Mentioned|p4|||Devonian-Carboniferous||||||
15099|Pertnjara Group|30238|4|Described|p68|||Upper Devonian to Carboniferous age||||||
15099|Pertnjara Group|30258|6|Mentioned|Fig.2|||Devonian - ?Carboniferous||||||
15099|Pertnjara Group|30544|6|Mentioned|p51|||||||||
15099|Pertnjara Group|30659|6|Mentioned|p87|||||||||
15099|Pertnjara Group|31566|4|Described|p230|||See also p231. Refers Wells et al. (1970).||||||22-NOV-06
15099|Pertnjara Group|31567|6|Mentioned|p273|||Refers Finke Group.||||||22-NOV-06
15099|Pertnjara Group|31707|6|Mentioned|Table 1|||||||||
15099|Pertnjara Group|31991|4|Described|p294|||Struct. geol. and geol.history.||||||22-NOV-06
15099|Pertnjara Group|32208|6|Mentioned|Map legend|Devonian|Devonian|||||||
15099|Pertnjara Group|32209|6|Mentioned|Map legend|Devonian|Devonian|||||||
15099|Pertnjara Group|32640|6|Mentioned|p235|||||||||
15099|Pertnjara Group|32865|6|Mentioned|p482|||||||||
15099|Pertnjara Group|33103|6|Mentioned|p25|||||||||
15099|Pertnjara Group|33306|6|Mentioned|p206|||||||||
15099|Pertnjara Group|33307|6|Mentioned|Fig.6|||||||||
15099|Pertnjara Group|33326|6|Mentioned|p449|||Fauna.||||||
15099|Pertnjara Group|33761|6|Mentioned|p146|||Devonian - Carb?||||||
15099|Pertnjara Group|33971|6|Mentioned|p30|||Refers stratigraphy.||||||
15099|Pertnjara Group|34111|5|Briefly described|Table 2|||Devonian - Carboniferous. See also pp5,6,14,16.||||||22-NOV-06
15099|Pertnjara Group|34186|6|Mentioned|Fig.3|||Devonian - Permian. See also Figs 4,8.||||||
15099|Pertnjara Group|34442|5|Briefly described|Table 1|||Devonian - Carboniferous||||||
15099|Pertnjara Group|34579|4|Described|Table 3|||Devonian - Carboniferous. See also pp16,17.||||||22-NOV-06
15099|Pertnjara Group|34580|4|Described|Table 1|||||||||
15099|Pertnjara Group|34810|6|Mentioned|p9|||Re ages.||||||
15099|Pertnjara Group|35102|6|Mentioned|Fig.2|||||||||
15099|Pertnjara Group|35628|6|Mentioned|Table 3|||||||||
15099|Pertnjara Group|36473|6|Mentioned|Map legend|Carboniferous|Devonian|Between Carboniferous and Devonian||||||
15099|Pertnjara Group|38319|6|Mentioned|p328|||||||||
15099|Pertnjara Group|38606|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
15099|Pertnjara Group|38885|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
15099|Pertnjara Group|39213|6|Mentioned|p15|||Molasse conglomerate. Fig.6||||||
15099|Pertnjara Group|39565|6|Mentioned|Fig.14|||||||||
15099|Pertnjara Group|39583|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
15099|Pertnjara Group|40201|5|Briefly described|p691|||||||||
15099|Pertnjara Group|40740|3|Fully described|p60|||Briefly described p6.||||||22-NOV-06
15099|Pertnjara Group|40810|5|Briefly described|p12|||||||||
15099|Pertnjara Group|40906|6|Mentioned|Fig.11|||||||||
15099|Pertnjara Group|41018|6|Mentioned|p234|||||||||
15099|Pertnjara Group|41039|6|Mentioned|Fig.2|||||||||
15099|Pertnjara Group|41125|6|Mentioned|p40|||See also fig.24.||||||
15099|Pertnjara Group|41190|6|Mentioned|p267|||||||||
15099|Pertnjara Group|41204|6|Mentioned|p14|||||||||
15099|Pertnjara Group|41224|6|Mentioned|Fig.2|||||||||
15099|Pertnjara Group|41270|6|Mentioned|p268|||||||||
15099|Pertnjara Group|41385|6|Mentioned|p363|||See also Fig.12||||||
15099|Pertnjara Group|41492|6|Mentioned|p158|||||||||
15099|Pertnjara Group|41708|6|Mentioned|Fig.1|||||||||
15099|Pertnjara Group|41717|6|Mentioned|Fig.2|||||||||
15099|Pertnjara Group|41723|6|Mentioned|Map legend|Late Devonian||||||||
15099|Pertnjara Group|41820|6|Mentioned|p6|||See also Fig.3||||||
15099|Pertnjara Group|42060|6|Mentioned|Fig.5 P140|||||||||
15099|Pertnjara Group|42141|6|Mentioned|Fig.3 P570|||||||||
15099|Pertnjara Group|42351|6|Mentioned|p46|||In the Amadeus Basin.||||||22-NOV-06
15099|Pertnjara Group|42354|6|Mentioned|p7|||||||||
15099|Pertnjara Group|42504|6|Mentioned|p80|||||||||
15099|Pertnjara Group|42564|6|Mentioned|p12|||In the Amadeus Basin.||||||22-NOV-06
15099|Pertnjara Group|42643|6|Mentioned|p32|||||||||
15099|Pertnjara Group|42699|5|Briefly described|map legend|Devonian||||||||
15099|Pertnjara Group|42845|5|Briefly described|p496|||||||||
15099|Pertnjara Group|42940|5|Briefly described|Plate 2|Devonian|Devonian|Sandstone, siltstone, conglomerate, limestone; fish fossils.  Age: 410-360Ma. Geological province: Amadeus Basin.||||||23-JAN-08
15099|Pertnjara Group|43035|4|Described|p23|||||||||
15099|Pertnjara Group|43105|5|Briefly described|Fig.3,p8.|||||||||
15099|Pertnjara Group|43225|5|Briefly described|Map Legend||Devonian|In the Amadeus Basin.||||||22-NOV-06
15099|Pertnjara Group|43503|6|Mentioned|32-50|Late Devonian|Middle Devonian|||||||
15099|Pertnjara Group|43631|6|Mentioned|p27|||||||||
15099|Pertnjara Group|43646|6|Mentioned|p553||Devonian|||||||
15099|Pertnjara Group|43647|6|Mentioned|p530|||||||||
15099|Pertnjara Group|43648|5|Briefly described|Fig.1,p488|||||||||
15099|Pertnjara Group|43649|5|Briefly described|fig.1,p454-455,459|||||||||
15099|Pertnjara Group|43749|6|Mentioned|p37|||||||||
15099|Pertnjara Group|43817|6|Mentioned|Fig.1,p62|||||||||
15099|Pertnjara Group|44133|5|Briefly described|p44|Devonian|Devonian|Includes: Parke Siltstone.||||||
15099|Pertnjara Group|44342|4|Described|p.6, Table 2|Carboniferous|Devonian|SG/53-5. Dev-Carbon.||||||
15099|Pertnjara Group|44343|14|Not recorded|map legend|Carboniferous|Devonian|Dev. to Carbon.||||||
15099|Pertnjara Group|44393|6|Mentioned|p.6,7,8,Fig.1|||Correlated with Finke Group.||||||
15099|Pertnjara Group|44395|14|Not recorded|p.9,10,12, Tb.2|||Devonian?||||||
15099|Pertnjara Group|44402|5|Briefly described|map legend|Carboniferous|Devonian|Includes Hermannsburg Sandstone and Parke Siltstone. Dev-Carb.||||||02-DEC-04
15099|Pertnjara Group|44433|14|Not recorded|map legend|||Devonian to Carboniferous.||||||
15099|Pertnjara Group|44484|14|Not recorded|p.5,8,9,11,Tb.1,Fig4|Carboniferous|Devonian|Defn on Tech.File F/53-13. Dev-Carb.||||||
15099|Pertnjara Group|44485|14|Not recorded|map legend|Carboniferous|Devonian|Includes Parke Silstone, Hermannsburg Sandstone. Dev-Carb.||||||
15099|Pertnjara Group|44493|4|Described|p.13, map|Carboniferous|Devonian|BLOODS RANGE sheet (G53-3). Dev-Carb.||||||22-NOV-06
15099|Pertnjara Group|44494|14|Not recorded|map legend|Carboniferous|Devonian|Devonian-Carboniferous.||||||
15099|Pertnjara Group|44495|4|Described|p.9, map|Carboniferous|Devonian|AYERS ROCK sheet (G52-8). Devonian-Carb.||||||22-NOV-06
15099|Pertnjara Group|44496|5|Briefly described|map legend|Carboniferous|Devonian|Red-brown siltstone.  Devonian-Carboniferous.||||||22-NOV-06
15099|Pertnjara Group|44497|4|Described|p.11, Table 2|Carboniferous|Devonian|SF/53-13. Dev-Carb.||||||
15099|Pertnjara Group|44498|14|Not recorded|map legend|Carboniferous|Devonian|Dev-Carb.||||||
15099|Pertnjara Group|44505|14|Not recorded|p.2,8, Fig.11|Carboniferous|Devonian|Dev-Carb.||||||
15099|Pertnjara Group|44506|14|Not recorded|map legend|Carboniferous|Devonian|Devonian-Carboniferous.||||||
15099|Pertnjara Group|45041|4|Described|p94|||See also ppP95-102. U.Dev. to L.Carb.||||||22-NOV-06
15099|Pertnjara Group|45097|6|Mentioned|p27|||See also p28. Brachiopods.||||||22-NOV-06
15099|Pertnjara Group|45140|5|Briefly described|p13-14, p64-65|Early Carboniferous|Devonian|Wells et al. (1970). Amadeus Basin. Non-marine: broad alluvial plain deposits. Similar lithology to Pedestal Beds. Equivalent to Angas Hills Beds.|||Parke Siltstone.|Correlated with Lucas Formation.||
15099|Pertnjara Group|45148|6|Mentioned|p20|||||||||
15099|Pertnjara Group|45153|6|Mentioned|p55|||||||||
15099|Pertnjara Group|45155|6|Mentioned|Fig.8|||||||||
15099|Pertnjara Group|45170|6|Mentioned|p9|||||||||
15099|Pertnjara Group|46829|6|Mentioned|Fig.2|||||||||
15099|Pertnjara Group|46830|6|Mentioned|p24|||||||||
15099|Pertnjara Group|46864|6|Mentioned|p40|||||||||
15099|Pertnjara Group|46928|6|Mentioned|Table 1|||||||||
15099|Pertnjara Group|47050|5|Briefly described|p240|||||||||
15099|Pertnjara Group|48890|4|Described|p.49|Carboniferous|Devonian|Ref on wrong card! Pertnjara Formation. See also Tables, Figs and Plates.||||||22-NOV-06
15099|Pertnjara Group|48963|6|Mentioned|p22|||||||||
15099|Pertnjara Group|50246|5|Briefly described|p20 Fig. 2|Carboniferous|Devonian|Includes the N'Dhala Member.||||||07-FEB-11
15099|Pertnjara Group|60547|5|Briefly described|Map Legend|Devonian|Devonian|Geological Province: Amadeus Basin.||||||03-JUN-05
15099|Pertnjara Group|61154|6|Mentioned|p34|||Geological Province: Amadeus Basin.||||||
15099|Pertnjara Group|61309|6|Mentioned|p15, p17|Devonian|Devonian|Deposited during the Alice Springs Orogeny. Geological Province: northern margin of Amadeus Basin. See also p25 Fig. 11.||||||06-FEB-08
15099|Pertnjara Group|61387|5|Briefly described|Map legend|Devonian|Silurian|Includes Mereenie Sandstone and undifferentiated rocks.  Geological Province: Amadeus Basin.||||||
15099|Pertnjara Group|61519|5|Briefly described|Map Legend|Devonian|Silurian|Geological Province: Amadeus Basin.||||||
15099|Pertnjara Group|62359|5|Briefly described|p544 Fig. 4a, p545||Devonian|Foreland basin unit. Geological Province: Amadeus Basin. See also p546 Fig. 6.||||||
15099|Pertnjara Group|62376|5|Briefly described|p18|Late Devonian|Late Devonian|Geological Province: Amadeus Basin.||||||09-FEB-10
15099|Pertnjara Group|62379|5|Briefly described|p7 Fig. 2|Devonian|Devonian|Geological Province: Amadeus Basin.||||||
15099|Pertnjara Group|62595|5|Briefly described|p29 Fig.6.|Carboniferous|Devonian|Ross River area.|||Includes N'Dahla Member.|||
15099|Pertnjara Group|62609|5|Briefly described|Map Legend|Carboniferous|Devonian|Sandstone, siltstone, conglomerate, some limestone. Overlies Mereenie Sandstone.||||||14-AUG-06
15099|Pertnjara Group|62620|5|Briefly described|Map Legend|Carboniferous|Devonian|Sandstone, siltstone, conglomerate, some limestone.||||||
15099|Pertnjara Group|63562|5|Briefly described|p338 fig 3, p352 fig 10, p350|Devonian|Devonian|Of Amadeus Basin. Upward-coarsening lacustrine, fluvial and alluvial fan deposits; thickening northwards.||||Overlies Mereenie Sandstone unconformably. Correlated to Dulcie Sandstone and Ethabuka Sandstone.|Upward-coarsening succession of lacustrine, fluvial and alluvial fan deposits.|
15099|Pertnjara Group|64334|5|Briefly described|p42|Devonian|Devonian|Deposition was synchronous with the main phase of the Alice Springs Orogeny.|||||Thick wedges of generally coarsening-upward non-marine clastic sediments.|
15099|Pertnjara Group|64778|6|Mentioned|p12-13, 33|Devonian|Devonian|N Amadeus Basin margin. Up to 3000m of clastics following the 375-340 Ma Pertnjara Movement (Alice Springs Orogeny).||||||
15099|Pertnjara Group|64809|5|Briefly described|p3, p6 Fig.4 |Late Devonian|Late Devonian||||Includes the Brewer Conglomerate, Hermannsburg Sandstone and Parke Siltstone.|||
15099|Pertnjara Group|64970|6|Mentioned|p719 Fig. 2|Devonian|Silurian|Geological Province: Amadeus Basin.||||||27-MAY-09
15099|Pertnjara Group|65074|6|Mentioned|p360|Devonian|Devonian|Amadeus Basin.||||Probably correlated with Lucas Formation and Pedestal beds (of Birrindudu Basin).||
15099|Pertnjara Group|65232|5|Briefly described|p72, p10 Fig 9.||Late Devonian|Includes Brewer Conglomerate at top. Thick succession of Late Devonian terrestrial sediments. Geol.Prov: Amadeus Basin.||||||09-FEB-10
15099|Pertnjara Group|65233|4|Described|p3 Fig. 2, p13|Late Devonian|Middle Devonian|Unconformable on Mereenie Sandstone. Geological province: Amadeus Basin. Written only as Pertnjara. Upward-coarsening foreland basin succession forming a thick clastic wedge - details incl.||||||07-FEB-11
15099|Pertnjara Group|65272|6|Mentioned|p319, p320 Fig.3|Late Devonian|Late Devonian|Deformed by the Alice Springs Orogeny.||||||
15099|Pertnjara Group|65309|5|Briefly described|p13, p16, pp18-19. |Devonian|Devonian|Central and northern Amadeus Basin. Interfingers with Finke Group. Ongoing uplift resulted in deposition of thicker and more extensive (than Finke Group), upward-coarsening sequence.|||Includes Parkes Siltstone.|||
15099|Pertnjara Group|65342|5|Briefly described|p3.|||Amadeus Basin. Max. thickness at least 194 m.||||Overlies Mereenie Sandstone.|Sandstone, siltstone, conglomerate, some limestone.|
15099|Pertnjara Group|65382|6|Mentioned|p711|Late Devonian|Middle Devonian|||||||
15099|Pertnjara Group|65489|6|Mentioned|p125|Devonian|Devonian|Amadeus Basin.||||||
15099|Pertnjara Group|66498|6|Mentioned|p45|||Amadeus Basin, central Australia.||N'Dhala Member.||||
15099|Pertnjara Group|66589|6|Mentioned|p180|Famennian|Givetian|Case studies cited; not visited in the field by the authors of this study.||||||
15099|Pertnjara Group|66767|5|Briefly described|p60|Devonian|Devonian|Amadeus Basin. Consists of a series of lacustrine, braided and meandering fluviatile and alluvial fan deposits during the Alice Springs Orogeny.|||Parke Siltstone, Hermannsburg Sandstone, Brewer Conglomerate.|Unconformably overlies Mereenie Sandstone.||
15099|Pertnjara Group|67326|5|Briefly described|p2|Late Devonian|Late Devonian|Amadeus Basin.|||Parke Siltstone, Hermannsburg Sandstone, Brewer Conglomerate.|Overlies Larapinta Group.||
15099|Pertnjara Group|67565|5|Briefly described|p5 Fig.3, p42.|||Amadeus Basin.|||Includes Parke Siltstone and Hermannsburg Sandstone.|Overlies Mereenie Sandstone.||03-DEC-15
15099|Pertnjara Group|67856|5|Briefly described|p338, 348|Late Devonian|Late Devonian||||Includes Parke Siltstone, Hermannsburg Sandstone, Brewer Conglomerate.|Unconformably overlies Mereenie Sandstone in N and E of basin.||
15099|Pertnjara Group|68298|6|Mentioned|p226|||Amadeus Basin. Unfossiliferous. Said to be similar age to Aztec Siltstone fauna, Antarctica.||||||
15099|Pertnjara Group|68323|6|Mentioned|p4 Fig.2|Late Devonian|Late Devonian|Amadeus Basin.|||Parke Siltstone, Hermannsburg Sandstone, Brewer Conglomerate.|||
15099|Pertnjara Group|69031|6|Mentioned|p9|Devonian|Devonian|Eastern Amadeus Basin.||||||
15099|Pertnjara Group|69427|6|Mentioned|p12:47-48|||Amadeus Basin. Synorogenic successions in this unit were progressively tilted as a result of S-directed thrusting in the Devonian.||||||12-JUL-16
15099|Pertnjara Group|69438|4|Described|p23:2-8, 37-40, 42, 46, 48, 50|Famennian|Givetian|Pritchard and Quinlan (1962). Northwest and north-central Amadeus Basin. Thins to the S. Devonian (Givetian- Frasnian)  fish fossils occur at several localities in basal Parke Siltstone. Min age constrained by Famennian spores in Brewer Conglomerate. Deposition was initiated by the Pertnjara Event, and the Group was mildly deformed, uplifted and eroded by the Brewer Event.|||Parke Siltstone, Hermannsburg Sandstone, Brewer Conglomerate.|Unconformably overlies Mereenie Sandstone. Correlative of, and interdigitates with, Finke Group.|A series of lacustrine, braided and meandering fluvial, and alluvial fan deposits.|13-SEP-18
15099|Pertnjara Group|69439|5|Briefly described|p24:11-12|Devonian|Devonian|Amadeus Basin. This unit's lithofacies resembles that of the Kerridy Sandstone (Ngalia Basin).|||Brewer Conglomerate.|||12-JUL-16
15099|Pertnjara Group|69449|6|Mentioned|p34:2 Fig.34.2|Devonian|Devonian|Eastern Amadeus Basin.||||||12-JUL-16
15099|Pertnjara Group|69453|6|Mentioned|p37:1|||Amadeus Basin.||||Stratigraphic equivalent to Pedestal beds.||12-JUL-16
15099|Pertnjara Group|69458|6|Mentioned|p42:8|Devonian|Devonian|Amadeus Basin.||||||12-JUL-16
15099|Pertnjara Group|69606|5|Briefly described|p4 fig 2|Carboniferous|Devonian|Deposited during the Alice Springs Orogeny. Amadeus Basin. Potential seal rock.||||Unconformably overlies the Mereenie Sandstone.|Shale, sandstone and conglomerate.|
15099|Pertnjara Group|69673|6|Mentioned|p67, p149 fig 120||||||Includes Parke Siltstone, Hermannsburg Sandstone, Brewer Conglomerate|Correlated with Finke Group||
15099|Pertnjara Group|69948|6|Mentioned|Fig.4.4|||Amadeus, Georgina and Wiso Basins. Syn-orogenic (Pertnjara Movement/Tabberabberan Orogeny).||||||
15099|Pertnjara Group|71088|6|Mentioned|p17-18|Devonian|Devonian|Amadeus Basin. This unit is locally folded and exposed near the type area of the Ligertwood beds.||||||03-MAY-23
15099|Pertnjara Group|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||siltstone, sandstone|
15099|Pertnjara Group|71268|5|Briefly described|1m_geologyp12_lut.csv||||||Includes Mereenie Sandstone.|||
15099|Pertnjara Group|71279|5|Briefly described|p355 Fig.2, p363, p374, p382 Tb.1|Late Devonian|Late Devonian|Amadeus Basin. Modelled magnetic properties.|||Parke Siltstone, Hermannsburg Sandstone, Brewer Conglomerate.|||
15099|Pertnjara Group|72360|5|Briefly described|Map legend|Devonian|Devonian|Of Amadeus Basin.|||Includes Brewer Conglomerate.||Includes calcareous siltstone, siltstone, sandstone.|09-SEP-19
15099|Pertnjara Group|72369|5|Briefly described|iii,p40|Late Devonian|Late Devonian|Of Amadeus Basin.|||Includes Hermannsburg Sandstone.|||
15099|Pertnjara Group|72374|5|Briefly described|iii,p3,23|||Of Amadeus Basin.|||Includes Hermannsburg Sandstone.|||
15099|Pertnjara Group|72476|6|Mentioned|p36 Fig.9|||Amadeus Basin. Time-temperature thermal history diagram.||||||
15099|Pertnjara Group|73085|6|Mentioned|p1|late Devonian|late Devonian||||Brewer Conglomerate, Hermannsburg Sandstone, Parke Siltstone|Underlain by Mereenie Sandstone. Equivalent to Finke Group (Larapinta Group).||
15099|Pertnjara Group|73279|6|Mentioned|p14-15|Devonian|Devonian|Amadeus Basin.|||Hermannsburg Sandstone|||
15122|Petrel Cove Formation|22581|5|Briefly described|Fig.2,p37|||Kanmantoo Group, Kanmantoo Basin. Overlies Balqhidder Formation. Overlain by Middleton Sandstone||||||
15122|Petrel Cove Formation|22643|5|Briefly described|p186, fig3,6,7|Early Cambrian|Early Cambrian|||||||
15122|Petrel Cove Formation|22840|6|Mentioned|Table1 P38|||||||||
15122|Petrel Cove Formation|23539|5|Briefly described|Fig 1 p 467|||||||||
15122|Petrel Cove Formation|23996|3|Fully described|p352|Cambrian|Cambrian|Of Kanmantoo Group.  Composed of fine-grained metapsammites and metasiltstones. Geological Province: Adelaide Fold Belt.||||||01-SEP-10
15122|Petrel Cove Formation|24465|4|Described|p357|Early Cambrian|Early Cambrian|Of Bollaparudda Subgroup (Kanmantoo Group).  Overlies Balquhidder Formation.||||||19-JAN-05
15122|Petrel Cove Formation|30380|6|Mentioned|Table 1|||Correlation||||||
15122|Petrel Cove Formation|30381|3|Fully described|p220|||See also p221.||||||15-FEB-07
15122|Petrel Cove Formation|32457|6|Mentioned|p90|||||||||
15122|Petrel Cove Formation|35255|6|Mentioned|Fig.8|||||||||
15122|Petrel Cove Formation|36836|6|Mentioned|Table 1|||||||||
15122|Petrel Cove Formation|38873|4|Described|Table 2|||||||||
15122|Petrel Cove Formation|40442|6|Mentioned|p17|||||||||
15122|Petrel Cove Formation|40454|5|Briefly described|p46|||||||||
15122|Petrel Cove Formation|40455|5|Briefly described|p71|||||||||
15122|Petrel Cove Formation|40856|6|Mentioned|Fig.23.6|||||||||
15122|Petrel Cove Formation|41947|6|Mentioned|Fig.2 P17|||||||||
15122|Petrel Cove Formation|42225|6|Mentioned|Fig.4 P224|||||||||
15122|Petrel Cove Formation|42270|6|Mentioned|p353|||||||||
15122|Petrel Cove Formation|42271|6|Mentioned|p381|||||||||
15122|Petrel Cove Formation|43200|6|Mentioned|p2||Cambrian|||||||
15122|Petrel Cove Formation|43703|6|Mentioned|Fig.1,p75|||||||||
15122|Petrel Cove Formation|43759|6|Mentioned|p445|||||||||
15122|Petrel Cove Formation|44133|5|Briefly described|p4 Fig. 7.2, 18|Middle Cambrian|Middle Cambrian|Geological Province: Stansbury Basin. Of the Kanmantoo Group. Overlies: Balquhidder Formation.||||||
15122|Petrel Cove Formation|60712|5|Briefly described| p28 Fig. 1, p30 Fig. 3|Early Cambrian|Early Cambrian|Of the Wattaberri Subgroup (Kanmantoo Group).||||||31-MAY-05
15122|Petrel Cove Formation|61307|5|Briefly described|p6 Fig. 3|Cambrian|Cambrian|Of the Kanmantoo Group. Intruded by Victor Harbor Granite. Geological Province: Adelaide Fold Belt. See also p18.||||||
15122|Petrel Cove Formation|64282|5|Briefly described|Map legend|Early Cambrian|Early Cambrian|Of the Kanmantoo Group. Geological Province: Kanmantoo Trough. Grey-black Bouma-like sandstone-mudstone couplets. Planar-bedded, fine- to medium-grained sandstone grading up to small-scale ripple x-laminated sandstone, siltstone and mudstone.||||||24-JUL-08
15122|Petrel Cove Formation|65375|5|Briefly described|p33.|Middle Cambrian|Middle Cambrian|||Unit in Kanmantoo Group.||Overlies Balquhidder Formation. Is overlain by Middleton Sandstone.||
15122|Petrel Cove Formation|65664|5|Briefly described|p1096, p1105, p1106 Fig.5|||||Of Bollaparudda Subgroup.||Overlies Balquhidder Formation. In tectonic contact with Middleton Sandstone.||09-MAY-12
15122|Petrel Cove Formation|65892|5|Briefly described|p9 Fig.4. |Middle Cambrian|Middle Cambrian|Fleurieu Peninsula.||Unit in Kanmantoo Group.||Overlies Balquhidder Formation. Is overlain by Middleton Sandstone.||
15122|Petrel Cove Formation|65921|5|Briefly described|p1, p2 (map legend).|Cambrian|Cambrian|Occurs at Pennington Bay along the beach and shore platform around to Point Reynolds.||Of the Kanmantoo Group.|||Sandstones and laminated muddy siltstones.|
15122|Petrel Cove Formation|68735|5|Briefly described|p235 Fig.3|Middle Cambrian|Middle Cambrian|Fleurieu Peninsula.||Of the Kanmantoo Group.||||10-APR-17
15122|Petrel Cove Formation|68993|6|Mentioned|p544 Fig.1|Middle Cambrian|Middle Cambrian|Fleurieu Peninsula.||Of the Kanmantoo Group.||||
15122|Petrel Cove Formation|73107|5|Briefly described|Map legend.|Early Cambrian|Early Cambrian|Kanmantoo Trough.||Kanmantoo Group.|||Grey-black Bouma-like sandstone-mudstone couplets. Planar-bedded fine to medium-grained sandstone grading up to small scale ripple cross-laminated sandstone, siltstone and mudstone.|
15122|Petrel Cove Formation|73188|6|Mentioned|p316|Early Cambrian|Early Cambrian|Mount Lofty Ranges.||Bollaparudda Subgroup, Kanmantoo Group|||Fine-grained turbidites.|
15132|Pfeiffer Adamellite|42884|2|Defined|p14|Early Ordovician|Late Cambrian|of Summerfield Intrusive Suite, see also Fig.2 P13. Reserved as Pfeiffer Monzonite.||||||
15170|Pidinga Formation|14227|5|Briefly described|Enclos. 2|Eocene|Eocene|Of Plantagenet Group. Presented as Pidinga.||||||07-FEB-11
15170|Pidinga Formation|22485|4|Described|p51 , Fig 2 & p53|Tertiary|Tertiary|Informally divided into upper and lower Pidinga Formation.||||||11-JUL-13
15170|Pidinga Formation|22587|6|Mentioned|p79 Fig.7|Middle Eocene|Middle Eocene|||||||
15170|Pidinga Formation|22613|3|Fully described|p19|Late Eocene|Middle Eocene|Eucla Basin.||||||21-OCT-08
15170|Pidinga Formation|22916|5|Briefly described|12|||||||||
15170|Pidinga Formation|23331|5|Briefly described|1088|Late Eocene|Middle Eocene|||||||
15170|Pidinga Formation|23343|5|Briefly described|39|Eocene|Eocene|||||||
15170|Pidinga Formation|23479|5|Briefly described|p26|Paleogene|Paleogene|Geological Province: Gawler Craton [??more likely shown overlying Gawler Craton rocks].||||||04-NOV-10
15170|Pidinga Formation|23488|5|Briefly described|p37, p39 Fig. 5|Middle Eocene|Middle Eocene|Estuarine sand and clay. Geological Province: Eucla Basin.||||||28-JUL-09
15170|Pidinga Formation|23533|5|Briefly described|p564 Fig 3|Late Eocene|Middle Eocene|Geological Province: Eucla Basin.||||||
15170|Pidinga Formation|23584|5|Briefly described|p31 Fig 17|Late Eocene|Early Eocene|Of Eundynie Group. Geological Province: Eucla Basin.||||||
15170|Pidinga Formation|23671|2|Defined|p1|Middle Eocene|Middle Eocene|Disconformably overlain by Wilson Bluff Limestone; probably also overlain by Nullarbor Limestone in marginal areas. Max. thickness: 86ft. Type section details included.||||||28-JUL-09
15170|Pidinga Formation|23792|5|Briefly described|Fig.D4|Early Eocene|Late Paleocene|Equivalent to Wobbegong supersequence. Unconformably overlies Potoroo Formation. Overlain by Wilsons Bluff Formation. Geological Province: Bight Basin.||||||21-JAN-16
15170|Pidinga Formation|23818|5|Briefly described|p174 Fig.84|Middle Eocene|Middle Eocene|Geological Province: Eucla Basin.||||||
15170|Pidinga Formation|23989|5|Briefly described|p54 Fig. 46|Middle Eocene|Early Eocene|Overlies Yilgarn Craton rocks||||||04-NOV-10
15170|Pidinga Formation|24057|5|Briefly described|p97|Tertiary|Tertiary|Geological Basin: Eucla Basin.||||||
15170|Pidinga Formation|24201|5|Briefly described|p373 Fig. 2|Ypresian|Thanetian|||||||
15170|Pidinga Formation|24338|5|Briefly described|p938 Fig. 2|Ypresian|Thanetian|Overlain by the Wilson Bluff Limestone and the Nullarbor Limestone. Unconformably overlies the Potoroo Formation. Formation is Fm in text. Geological Province: Bight Basin.||||||
15170|Pidinga Formation|24350|5|Briefly described|Fig. 4 Appdx|Ypresian|Thanetian|Equivalent to Wobbegong Supersequence.||||||21-JAN-16
15170|Pidinga Formation|24358|5|Briefly described|p32|Eocene|Eocene|Geological Province: Eucla Basin.||||||17-MAR-05
15170|Pidinga Formation|24396|4|Described|p218 Fig. 3, p221|Late Eocene|Middle Eocene|Lower part correlates with the Maralinga Formation of Clarke et al (2003). Flood zone clays and lignite, fluvial/estuarine channel sands, gravelly (carboneous) coarse sands. Overlain by Khasta Formation.  Overlies Gawler Craton rocks.||||||04-NOV-10
15170|Pidinga Formation|24397|4|Described|p240|Late Eocene|Late Eocene|Defined by Harris, 1966. Direct equivalent of Werrillup Fm. in WA. Formerly informally divided into upper and lower Pidinga Fm. Upper Pidinga Fm. included here; lower Pidinga Fm. now incl. in Maralinga Fm. Geological Province: Eucla Basin.||||||28-JUL-09
15170|Pidinga Formation|24553|5|Briefly described|p37, Fig. 7|Cenozoic|Cenozoic|Geological Province: Duntroon Sub-basin. Marine sands. Part of Wobbegong Supersequence.||||||07-FEB-11
15170|Pidinga Formation|24606|5|Briefly described|p956, p958 Fig. 3|Late Eocene|Middle Eocene|Geological Province: Eucla Basin||||||
15170|Pidinga Formation|24617|5|Briefly described|p114, p115 Fig. 3, p117, p125 Fig. 10|Eocene|Eocene|Geological Province: Eucla Basin. Conglomerates and sandstones which fine upwards into carbonaceous siltstones, mudstones and lignites.||||||
15170|Pidinga Formation|29591|6|Mentioned|p92|||||||||
15170|Pidinga Formation|29659|6|Mentioned|p8|||||||||
15170|Pidinga Formation|30807|6|Mentioned|p102|||Suggested map symbol||||||
15170|Pidinga Formation|30922|6|Mentioned|Map legend|Eocene|Eocene|||||||
15170|Pidinga Formation|31850|3|Fully described|p32|||||||||
15170|Pidinga Formation|32120|6|Mentioned|p276|||Eocene, fauna||||||
15170|Pidinga Formation|32203|6|Mentioned|p5|||Middle Eocene||||||
15170|Pidinga Formation|34308|5|Briefly described|p195|||Johannian||||||
15170|Pidinga Formation|34759|6|Mentioned|Fig.7|||Stratigraphy||||||
15170|Pidinga Formation|35080|6|Mentioned|p8|||||||||
15170|Pidinga Formation|35772|4|Described|Table 1|||||||||
15170|Pidinga Formation|36096|6|Mentioned|p212|||||||||
15170|Pidinga Formation|36213|6|Mentioned|p86|||||||||
15170|Pidinga Formation|37062|6|Mentioned|p187|||||||||
15170|Pidinga Formation|37132|5|Briefly described|p369|||||||||
15170|Pidinga Formation|37852|6|Mentioned|p2|||||||||
15170|Pidinga Formation|38068|5|Briefly described|p73|||See also Fig.7.||||||
15170|Pidinga Formation|38221|6|Mentioned|Fig.4|||Great Australian Bight Basin||||||
15170|Pidinga Formation|38602|6|Mentioned|Fig.2|||||||||
15170|Pidinga Formation|38604|6|Mentioned|Map legend|Eocene|Paleocene|Paleocene - Eocene||||||
15170|Pidinga Formation|38605|4|Described|p29|||See also Table 5.||||||
15170|Pidinga Formation|39322|6|Mentioned|Fig.3|||||||||
15170|Pidinga Formation|39923|6|Mentioned|p354|||||||||
15170|Pidinga Formation|39949|5|Briefly described|p274|||||||||
15170|Pidinga Formation|40003|5|Briefly described|Table 14|||||||||
15170|Pidinga Formation|40448|6|Mentioned|p41|||||||||
15170|Pidinga Formation|40912|6|Mentioned|Map legend|late Eocene|late Eocene|Latest Eocene||||||
15170|Pidinga Formation|40941|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
15170|Pidinga Formation|41505|6|Mentioned|p2|||||||||
15170|Pidinga Formation|41619|6|Mentioned|Map legend|late Eocene|middle Eocene|||||||
15170|Pidinga Formation|41626|6|Mentioned|p48|||||||||
15170|Pidinga Formation|42075|5|Briefly described|Fig.10 P250|||||||||
15170|Pidinga Formation|42086|3|Fully described|p2|||See also Fig.2.||||||21-OCT-08
15170|Pidinga Formation|42265|6|Mentioned|p2|||||||||
15170|Pidinga Formation|42356|5|Briefly described|Fig.15 P119|Eocene||See also Microfiche 7 p15, Fig.4, Fig.9, 10, 12, 13.||||||
15170|Pidinga Formation|42465|5|Briefly described|Map Legend|||||||||
15170|Pidinga Formation|42466|5|Briefly described|Map Legend|||||||||
15170|Pidinga Formation|42469|5|Briefly described|p39|||||||||
15170|Pidinga Formation|42475|3|Fully described|p19|||||||||
15170|Pidinga Formation|42545|5|Briefly described|p12|||||||||
15170|Pidinga Formation|42546|5|Briefly described|Map legend|Tertiary||||||||
15170|Pidinga Formation|42722|6|Mentioned|Tectonic sketch legend|Tertiary|Tertiary|||||||
15170|Pidinga Formation|42736|5|Briefly described|map legend|Tertiary||||||||
15170|Pidinga Formation|42816|4|Described|p22|||||||||
15170|Pidinga Formation|42959|5|Briefly described|p56|||see also p58 Fig.3||||||
15170|Pidinga Formation|43071|5|Briefly described|p16,Table 3|||||||||
15170|Pidinga Formation|43280|6|Mentioned|Map Legend||Tertiary|||||||
15170|Pidinga Formation|43814|6|Mentioned|Fig.3,p115|||||||||
15170|Pidinga Formation|43838|4|Described|p4, 9||Tertiary|Interfingers with Hampton Sandstone. Princess Royal Spongolite & Redmine Group overlies. 60m thick.||||||12-JUL-16
15170|Pidinga Formation|44133|5|Briefly described|p178|Early Oligocene|Middle Eocene|Geological Province: Eucla Basin. Thickness: 60m+.||||||
15170|Pidinga Formation|44145|6|Mentioned|p551  Table 4-27|Eocene|Eocene|Occurs near eastern margin of Eucla Basin in SA.||||Correlated with Hampton Sandstone, Werillip Formation.||
15170|Pidinga Formation|44695|5|Briefly described|Map Legend|Eocene|Eocene|(Middle-Late Eocene)||||||
15170|Pidinga Formation|44864|5|Briefly described|Map Legend||Eocene|||||||
15170|Pidinga Formation|44935|5|Briefly described|Map Legend|Late Eocene|Middle Eocene|||||||
15170|Pidinga Formation|46993|6|Mentioned|p262|||||||||
15170|Pidinga Formation|49060|5|Briefly described|Fig.15|||||||||
15170|Pidinga Formation|60497|5|Briefly described|p42|Early Oligocene|Eocene|Basal unit in the palaeochannels of the Eucla Basin.  Geological Province: Eucla Basin.||||||
15170|Pidinga Formation|60953|5|Briefly described|Map Legend|Eocene|Paleocene|Fluvial to estuarine and marine sand and lignite. Geological Province: Eucla Basin.||||||11-JUL-13
15170|Pidinga Formation|61108|5|Briefly described|map legend|Eocene|Paleocene|Fluvial to estuarine and marine sand and lignite. Geological Province: Eucla Basin.||||||
15170|Pidinga Formation|61155|5|Briefly described|p17|Late Eocene|Middle Eocene|Contains the Bring Member. Interfingers with Wilson Bluff Limestone. Age: ~45-36.5Ma. Max. thickness: 100m. Geological Province: Eucla Basin.||||||
15170|Pidinga Formation|61197|6|Mentioned|p481|Middle Eocene|Middle Eocene|Part of the infill within inset-valleys in the Yilgarn Craton.||||||
15170|Pidinga Formation|61544|5|Briefly described|p367 Fig.3. |Eocene|Paleocene|||||Is overlain by Nullarbor and Wilson Bluff Limestones.|Shallow marine sandstones.|
15170|Pidinga Formation|61630|6|Mentioned|p555 Fig. 3|Paleocene|Late Cretaceous|Geological Province: Bright and Duntroon Basins.||||||07-APR-09
15170|Pidinga Formation|61814|5|Briefly described|p22, p26|Middle Eocene|Middle Eocene|Coarse and fine-grained lignitic and siliciclastic deposit, mainly fluvial and estuarine; carbonaceous. Incised into weathered basement rock of underlying Gawler Craton.||||||04-NOV-10
15170|Pidinga Formation|61839|5|Briefly described|p227|Eocene|Eocene|Mainly fluvial carbonaceous sediments. Overlies Gawler Craton.||||||04-NOV-10
15170|Pidinga Formation|61856|5|Briefly described|p300 Fig.2, p304, p312|Late Eocene|Middle Eocene||||Includes Maralinga and Anthony Members.|||
15170|Pidinga Formation|62570|5|Briefly described|p582|Eocene|Eocene|Sediments overlying Observatory Hill Formation in Wilkinson 1 (core).||||||01-OCT-09
15170|Pidinga Formation|64340|5|Briefly described|p26 Tb. 5, p31|Middle Eocene|Middle Eocene|Of Eundynie Group.||||||
15170|Pidinga Formation|64646|6|Mentioned|p23 Fig. 3, p24 Fig. 4|Oligocene|Eocene|Includes Maralinga and Anthony Members. Geological Province: Gawler Craton.||||||08-FEB-10
15170|Pidinga Formation|65194|5|Briefly described|p136 Fig.4.37, p163-164, p170-172|Middle Eocene|Early Eocene|Oldest sediments in Lefroy Palaeovalley; also occurs in Musgrave region and Gawler Craton. Up to about 50m of fluvial sediments: silt, silty clay, lignite; minor gravel-rich sand bodies and pyrite. Interfingers with Hampton Sandstone. In Gawler Craton, grades laterally and vertically into Khasta Formation. Associated with uranium mineralisation. Is overlain unconformably by Garford Formation.||||||
15170|Pidinga Formation|65260|6|Mentioned|p26, p27 Fig.20|Middle Eocene|Middle Eocene|Of Eundynie Group. Lefroy Palaeochannel. Quartz sands, clay and lignite.||||||
15170|Pidinga Formation|65385|4|Described|pS127, pS129 Fig.3, Table 1|Late Eocene|Middle Eocene|Basal unit in the Garford paleovalley. Unconformably overlies Archean-Proterozoic  basement. Unconformably overlain by Garford Formation. Gravel, carbonaceous fine to coarse sand, silt, lignite.Terrestrial to estuarine-marine conditions.||||||26-MAR-13
15170|Pidinga Formation|65891|6|Mentioned|p221 Fig.5. |Paleogene|Paleogene|East Eucla Basin. Age shown as Bartonian to Priabonian.||||||
15170|Pidinga Formation|65922|5|Briefly described|p24, p25 Tb. 4, p45 Fig.10|Late Eocene|Middle Eocene|Interbedded, well-sorted, fine to coarse-grained carbonaceous sand and silt with minor lignite. Underlies Garford Formation conformably. Overlies weathered basement. Mainly restricted to Narlaby Palaeochannel.||||||
15170|Pidinga Formation|66131|6|Mentioned|p242 Fig.2|Eocene|Eocene|Age from Fig.2 - stratigraphic correlation chart.||||||
15170|Pidinga Formation|67462|5|Briefly described|Map legend.|Eocene|Eocene|Eucla Basin.|||Includes Maralinga and Anthony Members.|||
15170|Pidinga Formation|68128|5|Briefly described|p43, p71|Pliocene|Eocene|Gawler Craton.|||||Siltstone, carbonaceous; lignite; sand, carbonaceous. Palaeochannel fill.|01-FEB-23
15170|Pidinga Formation|68131|6|Mentioned|p71|Pleistocene|Pliocene|Flinders Island, Nuyts Domain, Gawler Craton.||||||
15170|Pidinga Formation|68715|6|Mentioned|p30 Fig.5|Bartonian|Lutetian|NW Gawler Craton, Eucla Basin.|||Anthony, Maralinga Members.|||07-APR-17
15170|Pidinga Formation|69004|4|Described|iii,  p19, p28, p32, p34, p38, p41, p115|Late Eocene|Middle Eocene|Eucla Basin. Sediments commonly form the basal infill sequence of many palaeovalleys in the Gawler-Eucla region. Informally divided into a "lower" and "upper" part on p34. Hosts groundwater aquifer in the Iluka Palaeovalley.||||Unconformably overlain by the Garford Formation. Overlain by the Khasta Formation and Narlaby Formation.|Variably oxidised carbonaceous sediments, fluvial sands and basal gravels.|
15170|Pidinga Formation|69297|5|Briefly described|p14 fig 2.4, p25 fig 2.9|Ypresian|Thanetian|Eyre, Ceduna and Duntroon Sub-basins. Deposited in shallow marine or shoreface environments. Good reservoir properties. See also p39 fig 2.14, p58, p60, p64.||||Unconformably overlies the Platypus Formation. Overlain by the Nullarbor Limestone and Wilsons Bluff Formation.|Sandstone and siltstone.|
15170|Pidinga Formation|69598|6|Mentioned|p9|Late Eocene|Middle Eocene||||Includes the Maralinga and Anthony Members.|Overlain by the Khasta Formation.||
15170|Pidinga Formation|69648|4|Described|p4,p21-22,p24,p27-28,p36,p38, map legend|Eocene|Eocene|King (1950, 1951) described sediments (Ifould Lake region) as the 'lignitic series' (occur in floor of some playa lakes), and overlying and outcropping 'lacustrine' clays and sands. Defined by Harris (1966). Harris (1966; see lithological log of Anderson, 1950) defined Formation on basis of SADME P5 drill hole at Ifould Lake on BARTON, adjacent to OOLDEA. Age: Middle to Late Eocene. Potential for placer gold deposits and other commodities. Thickness is variable: few to >50 m. This unit marks Tertiary base along most palaeochannels to NE, and within part of Eucla Basin. On OOLDEA: it unconformably overlies Cretaceous sediments of Bight Basin; toward Eucla Basin margin, it also overlies more indurated sediments of Officer Basin and crystalline basement of Gawler Craton in SE corner. Explored for coal, found lignites.||Burdunga Subgroup||Conformably overlain by/interfingers with Paling Member (Wilson Bluff Limestone); overlain by Ooldea Sand, Hampton Sandstone(conformably), Nullarbor Limestone, Garford Formation (unconformably).|Carbonaceous palaeochannel sediments (mud, sand and minor conglomerate); lignitic, and lacustrine clays and sands.|
15170|Pidinga Formation|69649|5|Briefly described|p31, p48|Eocene|Eocene|Harris (1966). Eucla Basin. Appears confined to topographic lows such as paleodrainage networks. c.80m thick. Sediment sourced fom Hiltaba Suite and Gawler Range Volcanics. Associated with uranium exploration.|||||Carbonaceous clay, silt and sand, with poor quality lignite.|
15170|Pidinga Formation|70067|5|Briefly described|Ceduna: Fig.2; p1. Regional: Fig.2|Ypresian|Thanetian|Bight Basin. Contains good quality sandstone reservoirs.||||Overlies Potoroo Formation.||
15170|Pidinga Formation|70772|6|Mentioned|p31, p41|||||||||
15170|Pidinga Formation|70778|5|Briefly described|p4|||Intersected in Nundroo 3 DDH.|||||Lignite; medium-coarse grained sand.|
15170|Pidinga Formation|71317|5|Briefly described|p143|Eocene|Eocene|||||Overlain by the Garford Formation.||
15170|Pidinga Formation|71789|6|Mentioned|p100|||||||||
15170|Pidinga Formation|71891|5|Briefly described|p6-p7, p30, p32-p40, p44-p52, p54-p55|Cenozoic|Cenozoic|Eucla Basin, Coompana Province. 30-60m thick. Interpreted to have been deposited in paleochannels and broader depressions.||||Unconformably overlies the Madura Formation. Overlain by the Hampton Sandstone.|Carbonaceous, terriginous clastic sedimentary rocks.|
15170|Pidinga Formation|72344|5|Briefly described|p4, p16,  p49, p61|||Eucla Basin. 30-60m thick package of carbonaceous terrigenous clastic sedimentary rocks deposited in topographically low settings. See also p84, p96, p160, p169.||||Overlain by the Hampton Sandstone.|Interbedded, well-sorted, fine to coarse-grained carbonaceous sands and silt with minor lignite. Flood zone clays and lignite, fluvial/estuarine channel sands, gravelly carbonaceous coarse sands.|
15170|Pidinga Formation|72465|5|Briefly described|p9, 17|Tertiary|Tertiary|Lowest unit in the Eucla Basin, Coompana Province. 30-60m thick.||||Is overlain by Hampton Sandstone.|Carbonaceous, terrigenous clastic sedimentary rocks: interbedded, well-sorted, fine- to coarse-grained carbonaceous sand and silt with minor lignite. Flood zone clays and lignite, fluvial/estuarine channel sands, gravelly (carbonaceous) coarse sands.|
15170|Pidinga Formation|72466|5|Briefly described|p9, 17|Tertiary|Tertiary|Benbow et al. (1995). Lowest unit in the Eucla Basin, Coompana Province. 30-60m thick.||||Overlies Madura Formation. Is overlain by Wilson Bluff Limestone and Hampton Sandstone.|Interbedded, well-sorted, fine- to coarse-grained carbonaceous sand and silt with minor lignite. Flood zone clays and lignite, fluvial/estuarine channel sands, gravelly (carbonaceous) coarse sands.|
15170|Pidinga Formation|72467|5|Briefly described|p9, 17|Tertiary|Tertiary|Lowest unit in the Eucla Basin, Coompana Province. 30-60m thick.||||Is overlain by Hampton Sandstone.|Carbonaceous, terrigenous clastic sedimentary rocks: interbedded, well-sorted, fine- to coarse-grained carbonaceous sand and silt with minor lignite. Flood zone clays and lignite, fluvial/estuarine channel sands, gravelly (carbonaceous) coarse sands.|
15170|Pidinga Formation|72468|5|Briefly described|p9, p17|||Eucla Basin. 30-60 m thick.||||Overlain by Hampton Sandstone.|Interbedded, well-sorted, fine to coarse-grained carbonaceous sand and silt with minor lignite. Flood zone clays and lignite, fluvial/estuarine channel sands, gravelly (carboneous) coarse sands.|
15170|Pidinga Formation|72469|5|Briefly described|p9, p17|||Eucla Basin. 30-60 m thick.||||Overlain by Hampton Sandstone.|Interbedded, well-sorted, fine to coarse-grained carbonaceous sand and silt with minor lignite. Flood zone clays and lignite, fluvial/estuarine channel sands, gravelly (carboneous) coarse sands.|
15170|Pidinga Formation|72470|5|Briefly described|p9, p18|||Eucla Basin. 30-60 m thick.||||Overlain by Hampton Sandstone.|Interbedded, well-sorted, fine to coarse-grained carbonaceous sand and silt with minor lignite. Flood zone clays and lignite, fluvial/estuarine channel sands, gravelly (carboneous) coarse sands.|
15170|Pidinga Formation|72471|5|Briefly described|p9|||Eucla Basin. 30-60 m thick.||||Overlain by Hampton Sandstone.|Interbedded, well-sorted, fine to coarse-grained carbonaceous sand and silt with minor lignite. Flood zone clays and lignite, fluvial/estuarine channel sands, gravelly (carboneous) coarse sands.|
15170|Pidinga Formation|72472|5|Briefly described|p9|||Eucla Basin. 30-60 m thick.||||Overlain by Hampton Sandstone.|Interbedded, well-sorted, fine to coarse-grained carbonaceous sand and silt with minor lignite. Flood zone clays and lignite, fluvial/estuarine channel sands, gravelly (carboneous) coarse sands.|
15170|Pidinga Formation|73099|5|Briefly described|Map legend.|Eocene|Eocene|Meramangye and Tallaringa Palaeochannels.||Burdunga Subgroup.||Overlies Bulldog Shale (Marree Subgroup). Is overlain by Garford Formation.|Green-grey, fine-grained quartz sandstone to grit, siltstone and claystone, carbonaceous in part; silcrete layers.|
15170|Pidinga Formation|73232|5|Briefly described|p8, p10, p18|Eocene|Eocene|Fluvial palaeovalley infill. Well known from palaeovalleys along the Eucla Basin northern margin. Tentatively correlated with the basal sandy unit of the Lindsay East Palaeovalley that has a thickness of 23 m in drillhole DH1a.|||||May include highly weathered, poorly to moderately sorted, coarse-grained, quartz-rich, kaolinitic sandstones that grade upward into consolidated, massive, more mature, moderately to well sorted, fine-grained, quartz-rich sandstones.|
15170|Pidinga Formation|73641|5|Briefly described|p4-5|||Basal unit in the Eucla Basin. 30-60m thick. Deposition in a palaeochannel and broader depression environment.||||Is overlain by Hampton Sandstone.|Interbedded, well-sorted, fine- to coarse-grained carbonaceous sand and silt; minor lignite, clays, channel sands, and gravelly coarse sands.|
15226|Pimba Formation|31532|4|Described|p322|||||||||
15226|Pimba Formation|33827|6|Mentioned|Table 1|||||||||
15226|Pimba Formation|33828|6|Mentioned|p11|||See also Table 1||||||
15279|Pinyinna beds|22506|6|Mentioned|p130 Fig.4|Cryogenian|Cryogenian|||||||
15279|Pinyinna beds|22647|6|Mentioned|Fig 1 on p 113|||||||||
15279|Pinyinna beds|22804|5|Briefly described|p441|Neoproterozoic|Neoproterozoic|||||||
15279|Pinyinna beds|22826|4|Described|p568|Neoproterozoic|Neoproterozoic|The Pinyinna beds are time equivalents of the Bitter Springs Formation in the southwest of the Basin.||||||
15279|Pinyinna beds|24301|4|Described|p14|Neoproterozoic|Neoproterozoic|Also referred to as Pinyinna Beds on p7 Tb.2 and p15. Lithology: siltstone and dolostone.  Geological Province: Amadeus Basin.||||||16-JUN-09
15279|Pinyinna beds|24302|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Grey to purple muscovite-quartz phyllite, thinly laminated; crenulated in places. Geological Province: Amadeus Basin.||||||16-JUN-09
15279|Pinyinna beds|24496|5|Briefly described|p21 Tb.2|Neoproterozoic|Neoproterozoic|Geological Province: Amadeus Basin.||||||
15279|Pinyinna beds|24497|5|Briefly described|Map legend|Early Paleocene|Neoproterozoic|Geological Province: Amadeus Basin.||||||
15279|Pinyinna beds|36701|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
15279|Pinyinna beds|41884|6|Mentioned|p70|||||||||
15279|Pinyinna beds|42940|6|Mentioned|p 1|||||||||
15279|Pinyinna beds|45155|6|Mentioned|p47|||||||||
15279|Pinyinna beds|45170|6|Mentioned|p5|||||||||
15279|Pinyinna beds|50286|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Geological Province: Amadeus Basin. Overlies Dean Quartzite.  Underlies Winnall beds, Inindia beds.||||||22-DEC-09
15279|Pinyinna beds|50321|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Geological Province: Amadeus Basin. Overlies Dean Quartzite. Underlies Inindia beds, Winnall beds.||||||23-NOV-06
15279|Pinyinna beds|60572|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Grey, quartz-muscovite phyllite.   Geological Province: Amadeus Basin.||||||23-DEC-09
15279|Pinyinna beds|60660|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Deformed basal sediments of Amadeus Basin.||||||22-FEB-05
15279|Pinyinna beds|60678|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Grey quartz-muscovite phyllite, crystalline dolostone, fine-grained sandstone,red, green and pale grey fissile siltstone, dolomitic siltstone.  Geological Province: Amadeus Basin.||||||11-JAN-05
15279|Pinyinna beds|60679|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Quartz-muscovite phyllite. Geological Province: Amadeus Basin.||||||
15279|Pinyinna beds|60683|4|Described|p25, p9 Tb. 1|Neoproterozoic|Neoproterozoic|Sequence of siltstone and dolomite - grey quartz-muscovite phyllite, crystalline dolostone.  Conformably overlie Pottoyu Granite and Dean Quartzite. Age: probably c.820Ma. Thickness: >100m. Geol. Prov: Amadeus Basin. Equiv. to Bitter Springs Formation.||||||20-APR-05
15279|Pinyinna beds|61154|5|Briefly described|p18, p5 Tb. 1|Neoproterozoic|Neoproterozoic|Grey to purple quartz-muscovite phyllite; crystalline dolostone; fine sst; red, green and pale fissile sltst; dolomitic sltst.  Dominated by phyllite, interlayered with dolostone and minor schists in the north and Petermann Ranges. Typ sect.thickness:250m||||||19-JUL-05
15279|Pinyinna beds|61306|5|Briefly described|p32|Proterozoic|Proterozoic|Geological Province: Amadeus Basin.||||||
15279|Pinyinna beds|61386|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Pinyinna  Geological Province: Amadeus Basin.||||||23-NOV-06
15279|Pinyinna beds|62376|5|Briefly described|p18|Late Proterozoic|Late Proterozoic|Geological Province: Amadeus Basin.||||||09-FEB-10
15279|Pinyinna beds|62379|5|Briefly described|p7 Fig. 2|Late Proterozoic|Late Proterozoic|Geological Province: Amadeus Basin.||||||
15279|Pinyinna beds|62989|6|Mentioned|p40|||Geological Province: Amadeus Basin.||||||07-FEB-08
15279|Pinyinna beds|65233|5|Briefly described|p3 Fig. 2|Neoproterozoic|Neoproterozoic|Geological province: Amadeus Basin.||||||07-FEB-11
15279|Pinyinna beds|65256|4|Described|piii, p5, p6 Tb.1, p8, p16-18, p21, p29|Cryogenian|Stenian|[Formerly Pinyinna Beds (in Forman 1966)]. Probably ~800-820 Ma. Sourced from local 1040-1080 Ma granites and volcanics. Phyllitic to schistose in character. >100m thick.||||Disconformably underlies Winnall beds, Inindia beds, Mount Currie Conglomerate; conformably overlies Dean Quartzite; correlative of the Bitter Springs Formation.|Red and grey shales, grey phyllite, crystalline brown and grey, foetid, stromatolitic dolostone.|19-MAY-14
15279|Pinyinna beds|67326|5|Briefly described|p2|Neoproterozoic|Neoproterozoic|Amadeus Basin.||||Overlies Dean Quartzite. Is overlain unconformably by Boord Formation.||
15279|Pinyinna beds|67856|4|Described|p341 tab 4-8, p338, 335, 337, 344, 348|Neoproterozoic|Neoproterozoic|Type section: Pinyinna Range 24o35'S, 129o51'E.  Stromatolites poorly preserved; age unknown. Misspelt as Pinnyinna beds in fig 4-30 p338.||||Overlain by Mount Currie Conglomerate (unconformably). equivalent to Bitter Springs Formation. Overlies Dean Quartzite (unconformably).|Sandstone, siltstone, limestone.|
15279|Pinyinna beds|68270|4|Described|p679,683|Tonian|Tonian|Amadeus Basin.||||Overlain unconformably by Inindia beds.||03-JUL-19
15279|Pinyinna beds|68323|6|Mentioned|p4 Fig.2|Neoproterozoic|Neoproterozoic|Amadeus Basin.||||||
15279|Pinyinna beds|69436|5|Briefly described|p21:4, 17-19|Neoproterozoic|Neoproterozoic|Olia Chain, Amadeus Basin. Involved in thin- and thick-skinned deformation by the Petermann Orogeny. At the top of this unit is a decollement surface below which basement and basal Amadeus Basin rocks were structurally interleaved.||||Is structurally interleaved with Dean Quartzite.||12-JUL-16
15279|Pinyinna beds|69437|5|Briefly described|p22:4-6|Cryogenian|Cryogenian|SW Amadeus Basin, Centralian A Superbasin. Supersequence 1.||||Overlies Dean Quartzite. Lateral equivalent of Bitter Springs Formation.||12-JUL-16
15279|Pinyinna beds|69438|2|Defined|p23:2-4, 9-10, 14-15, 18, 44, 52|Cryogenian|Cryogenian|Forman (1966), who described it as a metamorphosed equivalent of Bitter Springs Formation. SW Amadeus Basin. Type area in the Pinyinna Range, where it is over 200m thick. Appears as Pinyinna Beds on 23:4. Part of Supersequence 1 of the Centralian A Superbasin. Metamorphosed to amphibolite-grade facies, decreasing to greenschist facies to the N. Detrital zircon age populations suggest provenance from the Musgrave Province. Maximum age from SHRIMP U-Pb analyses of detrital zircons (Close et al., 2004); minimum age from intrusive dyke. Hosts uneconomic base metal occurrences.|Between 1058 +/- 31 Ma and c.820 Ma.|||Conformably (gradationally) overlies Dean Quartzite. Lateral equivalent of Bitter Springs Formation. Is intruded by an Amata Dolerite [equivalent] dyke.|Grey, brown and white, laminated micaceous siltstone, overlain by grey and pink laminated dolostone, sometimes stromatolitic, and grey limestone. Typically unmetamorphosed, but locally to lower amphibolite grade.|12-JUL-16
15279|Pinyinna beds|69673|5|Briefly described|p63, p80, p84, p88, p91|Neoproterozoic|Neoproterozoic|||||Overlies Dean Quartzite, correlated with Bitter Springs Formation|Micaceous siltstone overlain by laminated dolostone, sometimes stromatolitic; some limestone.|
15279|Pinyinna beds|70416|6|Mentioned|p65 Fig.2|Cryogenian|Cryogenian|Amadeus Basin.||||||
15279|Pinyinna beds|71088|6|Mentioned|p8|Neoproterozoic|Neoproterozoic|Amadeus Basin.||||||
15279|Pinyinna beds|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||dolostone, sandstone, siltstone, phyllite|
15279|Pinyinna beds|71268|5|Briefly described|1m_geologyp12_lut.csv||||||||Grey quartz-muscovite phyllite, crystalline dolostone, fine-grained sandstone, red, green and pale grey fissile siltstone, dolomitic siltstone. Dominated by phyllite, interlayered with dolostone and minor schists in the north and Petermann Ranges.|
15279|Pinyinna beds|71841|5|Briefly described|p1|Cryogenian|Cryogenian|Of Amadeus Basin.||||||
15279|Pinyinna beds|73085|6|Mentioned|p1|Tonian|Tonian|[Written as PINYINNA BEDS].||||Underlain by Dean Quartzite. Equivalent to Bitter Springs Group.||
15279|Pinyinna beds|73086|5|Briefly described|p: 3, 7, 15, 18, 30, 39, 148, 151, 154|||Amadeus Basin. Part of Supersequence I; deposited during the early sag phase of basin development. Restricted to sporadic exposures in the southwest of the basin. May correlate specifically with the Gillen Formation because of the conformable to transitional basal boundary with quartzite units.||||Correlates to Bitter Springs Group. Conformably underlain by Dean Quartzite|Shale and grey, crystalline, laminated, foetid and stromatolitic dolostone.|
15294|Pirramimma Sand Member|22525|6|Mentioned|p35,37||Eocene|upgradded to Pirramimmira Sandstone||||||
15294|Pirramimma Sand Member|22587|6|Mentioned|p79 Fig.7|Early Miocene|Early Oligocene|||||||
15294|Pirramimma Sand Member|30250|2|Defined|p2|early Miocene|late Eocene|Late Eocene to Early Miocene||||||
15294|Pirramimma Sand Member|35689|2|Defined|p23|early Miocene|Oligocene|Late Eocene to Early Miocene||||||
15294|Pirramimma Sand Member|36127|6|Mentioned|p7|||||||||
15294|Pirramimma Sand Member|36244|6|Mentioned|p2|||Defined by Cooper 1977, 1979.||||||
15294|Pirramimma Sand Member|39351|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
15294|Pirramimma Sand Member|40453|6|Mentioned|Fig.6|||||||||
15294|Pirramimma Sand Member|41495|6|Mentioned|Table 5|||||||||
15294|Pirramimma Sand Member|41513|6|Mentioned|Fig.4|||||||||
15294|Pirramimma Sand Member|41520|6|Mentioned|Fig.4|||||||||
15294|Pirramimma Sand Member|70660|5|Briefly described|p8, p46|Miocene|Eocene|[Obsolete, see the Pirramimma Sandstone.]||||||
15317|Platypus Formation|22485|4|Described|p51 , Fig 2|Late Cretaceous|Late Cretaceous|||||||
15317|Platypus Formation|22663|6|Mentioned|S97-1 and 2 p3|||||||||
15317|Platypus Formation|23792|5|Briefly described|Fig.D4|Cenomanian|Cenomanian|Equivalent to White Pointer supersequence. Overlies Ceduna Formation. Overlain by Wigunda Formation. Geological Province: Bight Basin.||||||04-MAY-05
15317|Platypus Formation|24201|5|Briefly described|p373 Fig. 2|Cenomanian|Cenomanian|||||||
15317|Platypus Formation|24338|5|Briefly described|p938 Fig. 2|Cenomanian|Cenomanian|Overlain by the Wigunda Formation. Overlies the Ceduna Formation. Formation is Fm in text. Geological Province: Bight Basin.||||||
15317|Platypus Formation|24350|5|Briefly described|Fig. 4 Appdx|Cenomanian|Cenomanian|Part of White Pointer Supersequence||||||
15317|Platypus Formation|24443|5|Briefly described|Fig.7|Cenomanian|Cenomanian|Overlies Ceduna Formation. Overlain by Wigunda Formation. Geological Province: Bight Basin.||||||
15317|Platypus Formation|24553|5|Briefly described|p36, Figs. 7,8 and 10|Early Cretaceous|Early Cretaceous|Geological Province: Duntroon Sub-basin. Highly porous rocks. Significant oil shows. Appears in both the Blue Whale and White Pointer Supersequences.||||||07-FEB-11
15317|Platypus Formation|34759|6|Mentioned|Fig.7|||Stratigraphy||||||
15317|Platypus Formation|36244|6|Mentioned|p2|||Refers Fraser & Tilbury 1979.||||||
15317|Platypus Formation|38221|6|Mentioned|Fig.4|||Great Australian Bight Basin||||||
15317|Platypus Formation|42545|2|Defined|p8|Cenomanian||||||||
15317|Platypus Formation|43026|5|Briefly described|Table 1,p586|||||||||
15317|Platypus Formation|43672|6|Mentioned|p330|Cenomanian|Albian|||||||
15317|Platypus Formation|43814|6|Mentioned|Fig.3,p115|||||||||
15317|Platypus Formation|44133|5|Briefly described|p141|Cenomanian|Albian|Thickness: 394m. Disconformably overlies: Ceduna Formation. Conformably overlain by the Wombat Sandstone Member.||||||
15317|Platypus Formation|49060|5|Briefly described|Fig.15|||||||||
15317|Platypus Formation|61544|5|Briefly described|p367 Fig.3, p374.|Cenomanian|Cenomanian|Bight Sub-basin. Post-rift fluvio-deltaic source rocks, primarily with gas source potential.||||Overlies Ceduna Formation. Is overlain by Wigunda Formation.||
15317|Platypus Formation|61630|6|Mentioned|p555 Fig. 3, p556, p557, p558|Late Cretaceous|Late Cretaceous|Geological Province: Bright and Duntroon Basins.||||||07-APR-09
15317|Platypus Formation|69297|5|Briefly described|p14 fig 2.4, p25 fig 2.9|Turonian|Cenomanian|Eyre, Ceduna and Duntroon Sub-basins. Deposited in lower and upper deltal plains. Good reservoir properties. See also p39 fig 2.14, p58, p60, p64.||||Overlies the Ceduna Formation. Unconformably overlain by the Pidinga Formation. Equivalent to the Toondi Formation.|Sandstone and shale.|
15317|Platypus Formation|70067|5|Briefly described|Ceduna: Fig.2. Regional: Fig.2|Cenomanian|Cenomanian|Bight Basin.||||Overlies Ceduna Formation. Is overlain by Wigunda Formation.||
15331|Plug Range granite gneiss|36627|6|Mentioned|p81|||||||||
15331|Plug Range granite gneiss|38108|6|Mentioned|Table 1|||||||||
15365|Point Addis Limestone|22626|6|Mentioned|446 fig 10, 447|Late Oligocene|Late Oligocene|Geol province East Otway Basin. Overlying unit Puebla Clay, underlying unit Angahook Formation||||||
15365|Point Addis Limestone|23768|5|Briefly described|p28 Fig.5|Early Miocene|Early Miocene|In the Torquay/Geelong area.  Presented as Pt Addis only in figure.  See also p7, p103.||||||30-MAR-05
15365|Point Addis Limestone|23778|6|Mentioned|p668|||||||||
15365|Point Addis Limestone|24551|5|Briefly described|p313|||Of the Torquay Group.||||||
15365|Point Addis Limestone|31245|6|Mentioned|p74|||Fauna. Oligocene.||||||
15365|Point Addis Limestone|32552|6|Mentioned|p184|||Janjukian||||||
15365|Point Addis Limestone|32601|6|Mentioned|p674|||Equinoid source material||||||
15365|Point Addis Limestone|33155|5|Briefly described|p118|||||||||
15365|Point Addis Limestone|34421|6|Mentioned|p261|||||||||
15365|Point Addis Limestone|36499|6|Mentioned|p34|||||||||
15365|Point Addis Limestone|37311|6|Mentioned|p49|||||||||
15365|Point Addis Limestone|37602|4|Described|p645|||||||||
15365|Point Addis Limestone|41043|5|Briefly described|p96|||||||||
15365|Point Addis Limestone|41519|6|Mentioned|p168|||||||||
15365|Point Addis Limestone|41547|6|Mentioned|Fig.4|||||||||
15365|Point Addis Limestone|42371|6|Mentioned|p35, p36|Janjukian||||||||
15365|Point Addis Limestone|42655|6|Mentioned|p39|||Member of Jan Juc Formation||||||
15365|Point Addis Limestone|43702|6|Mentioned|Fig.2,p398|Miocene|Late Oligocene|||||||
15365|Point Addis Limestone|60299|5|Briefly described|p228 Tb.5|Oligocene|Oligocene|Age: 26 Ma. Palaeopole position given.||||||
15365|Point Addis Limestone|60563|5|Briefly described|p47|Oligocene|Oligocene|Bioclastic calcarenites.||||||
15365|Point Addis Limestone|60785|5|Briefly described|p184 Fig.1, pp189-190.   |Chattian|Chattian|Of the Torquay/Port Phillip Basins. Has yielded a variety of fossil cetacean elements at different locations.|||||Yellow sandy bryozoal calcarenite. Ferruginous intraclastic conglomerate with abraded shelly and vertebrate skeletal components.|
15365|Point Addis Limestone|61186|6|Mentioned|p93|Miocene|Oligocene|Victorian dimension stone.||||||
15365|Point Addis Limestone|62899|6|Mentioned|p51|Early Miocene|Late Oligocene|||||||
15365|Point Addis Limestone|63739|5|Briefly described|p51|Early Miocene|Late Oligocene|Contains ostracod assembalges (Hermanites sp.).||||||01-JUL-08
15365|Point Addis Limestone|65316|4|Described|p595, p598, p597 Fig 2, p601-603|Chattian|Rupelian|Lower section age equivalent to Jan Juc Marl.  Thought correlative of Clifton Formation. Abundant shelly fossils; distinctive marine assemblage close to the contact with Angahook Formation.|24.24 +1.3 / -1.2 Ma at base.|Of Torquay Group.||Unconformably overlies Angahook Formation; conformably overlain by Puebla Clay.|Marine calcarenite and sandy marl.|23-APR-12
15365|Point Addis Limestone|67061|5|Briefly described|p546.||||24.24 Ma.|Unit in Torquay Group.||||
15365|Point Addis Limestone|69297|6|Mentioned|p98|Chattian|Chattian|||Torquay Group||Overlies the Angahook Formation. Overlain by the Jan Juc Formation.|Limestones.|
15365|Point Addis Limestone|70942|5|Briefly described|p121, 119|||||||||
15383|Point Turton Limestone|23768|6|Mentioned|p103|Janjukian|Janjukian|||||||
15383|Point Turton Limestone|31850|6|Mentioned|p37|||Refers Ludbrook (1963)||||||
15383|Point Turton Limestone|35689|6|Mentioned|Fig.33|||Stratigraphic correlation, St.Vincent Basin.||||||
15383|Point Turton Limestone|40217|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
15383|Point Turton Limestone|42731|5|Briefly described|map legend|Miocene|Oligocene|||||||
15383|Point Turton Limestone|44133|5|Briefly described|p153 Fig. 10.2|Early Miocene|Late Oligocene|Geological Province: Pirie Basin. Interfingers with Melton Limestone.||||||
15383|Point Turton Limestone|44691|4|Described|map legend|Miocene|Oligocene|Defn on Tech.File (I/53-12). Oligocene-Miocene.||||||
15383|Point Turton Limestone|60958|5|Briefly described|Map Legend|Miocene|Eocene|Red-brown, coarse-grained, trough cross-bedded sandstone, silty medium-grained sandstone and upper bryozoal limestone. Geological Province: Saint Vincent Basin.||||||
15383|Point Turton Limestone|61121|5|Briefly described|Map legend|Miocene|Eocene|Red-brown, coarse-grained, trough cross-bedded sandstone, silty medium-grained sandstone and upper bryozoal limestone; fossils including 'Victoriella'. Geological Province: St. Vincent Basin.||||||06-JUN-05
15383|Point Turton Limestone|64282|5|Briefly described|Map legend|Miocene|Oligocene|Geolocial Province: St Vincent Basin. Red-brown, coarse-grained, trough cross-bedded sandstone, silty medium-grained sandstone and upper bryozoal limestone; fossils include Victoriella.||||||24-JUL-08
15383|Point Turton Limestone|65375|4|Described|p37, p50. |Miocene|Oligocene|Thickness to 16m. The bryozoan limestone correlates with Port Willunga Formation and Melton Limestone. Offshore seismic survey suggests deposition in a graben structure formed by reactivation of Warooka Fault zone.||||Unconformably overlies Cape Jervis Formation.|Basal coarse-grained, red-brown, well-sorted, thin-layered sandstone; silty medium-grained sandstone; upper bryozoan limestone.|
15383|Point Turton Limestone|73107|5|Briefly described|Map legend.|Miocene|Oligocene||||||Red-brown, coarse-grained, trough cross-bedded sandstone, silty medium-grained sandstone and upper bryozoal limestone. Fossils, including Victoriella.|
15383|Point Turton Limestone|73292|6|Mentioned|p954|Miocene|Oligocene|Equivalent of the Port Willunga Formation.||||||
15393|Polda Formation|23792|5|Briefly described|Fig.D4|Kimmeridgian|Callovian|Equivalent to Sea Lion supersequence. Geological Province: Bight Basin.||||||
15393|Polda Formation|24201|5|Briefly described|p373 Fig. 2|||Name used to describe unnamed equivalent of Polda Formation.||||||
15393|Polda Formation|24338|5|Briefly described|p938 Fig. 2|Kimmeridgian|Callovian|Overlain by the Echidna Formation. Formation is Fm in text. Geological Province: Bight Basin. Is unnamed in text but is referred to as the Polda Formation Equivalent.||||||
15393|Polda Formation|24350|5|Briefly described|Fig. 4 Appdx|Late Jurassic|Middle Jurassic|Mentioned only in terms of an unnamed equivalent, in the Sea Lion Supersequence.||||||
15393|Polda Formation|24443|6|Mentioned|Fig.7|||Used as Polda Formation equivalent.||||||
15393|Polda Formation|24553|5|Briefly described|p36|Jurassic|Jurassic|Geological Province: Polda Trough.||||||07-FEB-11
15393|Polda Formation|29856|6|Mentioned|p37|||||||||
15393|Polda Formation|35672|6|Mentioned|p11|||||||||
15393|Polda Formation|37850|2|Defined|p13|Late Jurassic|Late Jurassic|||||||
15393|Polda Formation|37851|6|Mentioned|p10|||||||||
15393|Polda Formation|39211|6|Mentioned|Fig.42|||||||||
15393|Polda Formation|40445|6|Mentioned|p52|||||||||
15393|Polda Formation|40448|4|Described|p41|||||||||
15393|Polda Formation|40673|6|Mentioned|p11|||||||||
15393|Polda Formation|41218|6|Mentioned|p328|||||||||
15393|Polda Formation|41363|6|Mentioned|p16|||||||||
15393|Polda Formation|42648|5|Briefly described|p48|||||||||
15393|Polda Formation|42716|5|Briefly described|Map legend|Jurassic||||||||
15393|Polda Formation|42738|5|Briefly described|map legend|Jurassic||||||||
15393|Polda Formation|43026|5|Briefly described|Table 5,p591|||||||||
15393|Polda Formation|43049|4|Described|p21|||||||||
15393|Polda Formation|43052|5|Briefly described|Table 2.1|||||||||
15393|Polda Formation|43053|5|Briefly described|Map Legend|Jurassic|Jurassic|Fluvial sandstone and conglomerate.||||||25-MAY-05
15393|Polda Formation|43258|5|Briefly described|Map Legend||Jurassic|||||||
15393|Polda Formation|43298|5|Briefly described|Map Legend||Jurassic|||||||
15393|Polda Formation|44133|4|Described|p72 Fig. 8.11, 131|Late Jurassic|Middle Jurassic|Geological Province: Polda Basin. Overlies Kilroo Formation. Unconformably overlies: Coolardie Formation. Disconformably overlain by the Poelpena Formation. Type section ~86m thick.||||||11-JUL-13
15393|Polda Formation|44145|6|Mentioned|p549  |||South Australian rocks broadly similar to Loongana Formation.||||||
15393|Polda Formation|60953|5|Briefly described|Map Legend|Jurassic|Jurassic|Fluvial sandstone and conglomerate.||||||
15393|Polda Formation|61108|5|Briefly described|map legend|Jurassic|Jurassic|Fluvial sandstone and conglomerate.||||||
15393|Polda Formation|61544|6|Mentioned|p367 Fig.3. |||Is equivalent to the unit underlying Echidna Formation in the Ceduna Sub-basin.||||||
15393|Polda Formation|62893|4|Described|Map Legend, p18-20, p22, p29|Late Jurassic|Late Jurassic|Polda Basin (only). Fluviatile to lacustrine sequence. Type section is in SADME Polda 1 drillhole where it is 86 m thick. Thickness ranges from 11 m to 282 m. Three informal members were described by Gatehouse and Cooper (1982) from the type section, although the sections change greatly between holes. Correlates with the Late Jurassic J6 microflora of Evans (1966). Overlies Archaean-Proterozoic basement rocks on the southern basin margin.||||Unconformably underlain by Coolardie Formation. Disconformably overlain by Poelpena Formation.|Grey, brown and black clayey sand, grey to dark grey carbonaceous silt, and clay beds with interlayered lignite and coal and also quartz and kaolin-rich cobbly conglomerate.|
15393|Polda Formation|65376|6|Mentioned|p38, p41.|Jurassic|Jurassic|||||||
15393|Polda Formation|68135|5|Briefly described|p52 fig 2b |Oxfordian|Callovian||||||Interbedded siltstone and sandstone.|14-SEP-17
15393|Polda Formation|69297|6|Mentioned|p58|Early Cretaceous|Middle Jurassic|||||||
15393|Polda Formation|71037|6|Mentioned|p21 Fig.1|Jurassic|Jurassic|Shown only on 'Outcropping geology and mineral deposits of northern Eyre Peninsula' map p21 Fig.1.||||Shown as younger than Tent Hill Formation and older than unnamed undifferentiated Tertiary sediments.||
15393|Polda Formation|71559|6|Mentioned|p15 Fig 1|Jurassic|Jurassic|Geological province: Gawler Craton.||||||
15393|Polda Formation|71859|6|Mentioned|p6, p18|Jurassic|Jurassic|||||||
15393|Polda Formation|73130|6|Mentioned|[poster] Fig.1|Jurassic|Jurassic|||||||28-OCT-22
15430|Poolamacca Group|22553|6|Mentioned|p77|||part of the Adelaidean sequence||||||
15430|Poolamacca Group|22772|5|Briefly described|p53,Fig13.1p63|Cryogenian|Cryogenian|||||||
15430|Poolamacca Group|22857|5|Briefly described|p64, Tb. 13.1 (insert p70-71)|Neoproterozoic|Neoproterozoic|Geological Province: Adelaide Fold Belt. See also p398 App. 1 Tb. A1.3.||||||
15430|Poolamacca Group|29864|6|Mentioned|p263|||||||||
15430|Poolamacca Group|30261|4|Described|Table 1|||Willouran age||||||
15430|Poolamacca Group|31012|6|Mentioned|p8|||Adelaidean. Lithology.||||||
15430|Poolamacca Group|32671|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
15430|Poolamacca Group|33004|6|Mentioned|p134|||||||||
15430|Poolamacca Group|34812|6|Mentioned|p4|||||||||
15430|Poolamacca Group|35199|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
15430|Poolamacca Group|36411|6|Mentioned|p269|||Refs Cooper et al. 1978 for definition.||||||
15430|Poolamacca Group|36733|6|Mentioned|Table 5|||||||||
15430|Poolamacca Group|37854|6|Mentioned|Table 1|||||||||
15430|Poolamacca Group|37931|6|Mentioned|p531|||||||||
15430|Poolamacca Group|38157|6|Mentioned|Table II|||||||||
15430|Poolamacca Group|38794|5|Briefly described|p234|||||||||
15430|Poolamacca Group|38969|6|Mentioned|p199|||||||||
15430|Poolamacca Group|39214|6|Mentioned|Table 1|||||||||
15430|Poolamacca Group|39652|6|Mentioned|p78|||||||||
15430|Poolamacca Group|39885|6|Mentioned|p427|||||||||
15430|Poolamacca Group|40294|6|Mentioned|Table 2|||||||||
15430|Poolamacca Group|40595|6|Mentioned|p77|||||||||
15430|Poolamacca Group|41403|5|Briefly described|p50|||||||||
15430|Poolamacca Group|41405|6|Mentioned|p203|||||||||
15430|Poolamacca Group|42223|6|Mentioned|Fig.2 P36|||||||||
15430|Poolamacca Group|42531|5|Briefly described|Map legend|Adelaidean||||||||
15430|Poolamacca Group|42982|5|Briefly described|Table 1,p333|||||||||
15430|Poolamacca Group|43263|6|Mentioned|Map Legend||Neoproterozoic|||||||
15430|Poolamacca Group|43265|5|Briefly described|Map Legend||Neoproterozoic|||||||
15430|Poolamacca Group|43268|5|Briefly described|Map Legend||Neoproterozoic|||||||
15430|Poolamacca Group|43269|5|Briefly described|Map Legend||Neoproterozoic|||||||
15430|Poolamacca Group|44093|5|Briefly described|p139 App. 1|Early Paleozoic|Neoproterozoic|Geological Province: Adelaide Fold Belt.||||||07-NOV-08
15430|Poolamacca Group|62724|5|Briefly described|p17 Fig. 4, p21|Willouran|Willouran|Includes Wilangee Volcanics, Boco Formation, Christine Judith Conglomerate and Lady Don Quartzite. Geological Province: Broken Hill Domain/Curnamona Province (NSW).||||||07-FEB-11
15430|Poolamacca Group|63489|5|Briefly described|Map legend|Adelaidean|Adelaidean|New South Wales equivalent of Poolamacca Group of South Australia. Basal quartzite and conglomerate, carbonate and basalt.||||||10-SEP-07
15430|Poolamacca Group|70000|5|Briefly described|p33-34, p39|Tonian|Tonian|Represents initial sedimentation in the Adelaide Rift Complex. Uplifted and eroded during Sturtian tectonism.|||Includes Pintapah and Wendalpa Subgroups.|Unit in Adelaide Rift Complex.|Fluviatile to shallow marine, mature sandstone and lesser conglomerate; followed by stromatolitic limestone; then a cover of continental flood basalt.|
15430|Poolamacca Group|70015|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Mineral deposits (if any) are shown.|||Includes Pintapah and Wendalpa Subgroups.||Quartzite to quartz-rich conglomerate overlain by sandstone, limestone and basalt.|
15430|Poolamacca Group|72461|5|Briefly described|p13, p16||||||Includes the Pintapah Subgroup and the Wendalpa Subgroup.|||
15442|Poolowanna Formation|12597|5|Briefly described|p498-499, p501|||NW Eromanga Basin. 200m thick. Appears as Poolawanna Formation on p501.||||Grades laterally into, and is overlain by, Algebuckina Sandstone. Is conformably overlain by Hutton Sandstone.|Mainly fluvial sequence of interbedded fine-grained sub-labile sandstone, siltstone and mudstone, with minor coal seams generally <0.5m thick.|
15442|Poolowanna Formation|13497|5|Briefly described|p89, p104, p112, p114|Early Jurassic|Early Jurassic|Eromanga Basin. Deposited in a high-sinuosity fluvial, overbank or lacustrine environment. Oil and gas reservoir. See also p115 fig 6.33, p119, p130, p138 fig 8.17, p141, p149-p151, p153,  p167, p170, p216.||||Overlies the Patchawarra Formation. Unconformably overlies the Tinchoo Formation. Disconformably overlain by the Cuddapan Formation.  Overlain by the Hutton Sandstone.|Sandstones, siltstone, shale and minor coal.|
15442|Poolowanna Formation|13516|6|Mentioned|p167 fig 10, p171 fig 12, p172|Middle Jurassic|Early Jurassic|In Eromanga Basin.||||||
15442|Poolowanna Formation|22839|6|Mentioned|P33|||||||||
15442|Poolowanna Formation|22883|5|Briefly described|P31, Fig2||Early Jurassic|Overlying unit is Algebuckina Sandstone||||||
15442|Poolowanna Formation|23054|6|Mentioned|Fig5p22|Aalenian|Sinemurian|||||||
15442|Poolowanna Formation|23154|5|Briefly described|Map Legend|Early Jurassic|Early Jurassic|Geological Province - Eromanga Basin.||||||
15442|Poolowanna Formation|23155|4|Described|p25|Early Jurassic|Early Jurassic|Early Jurassic in age from palynological evidence. Unit contains coal seams (<1m typically) and has carbonised plant fossils preserved on bedding surfaces.  On STRZELECKI the unit is overlain by Hutton Sandstone (conformity).||||||16-SEP-08
15442|Poolowanna Formation|23375|4|Described|Fig2 p265|Aalenian|Sinemurian|In the Eromanga Basin.||||||17-JAN-08
15442|Poolowanna Formation|23982|5|Briefly described|p58 Fig.18|||Geological Province: Eromanga Basin.||||||
15442|Poolowanna Formation|24092|5|Briefly described|p8 Fig.3|||Geological Province: Eromanga Basin.||||||
15442|Poolowanna Formation|24204|5|Briefly described|p266, 263 Fig.4, p266 Fig.7|Early Jurassic|Early Jurassic|Overlain unconformably by Algebuckina Formation. Geological Province: Eromanga Basin.||||||
15442|Poolowanna Formation|24210|5|Briefly described|p132, p133 Fig. 2|Middle Jurassic|Early Jurassic|Comprises fluvial sandstones, interbedded with shales and discontinuous, thin coals. Geological Province: Eromanga Basin.||||||16-SEP-08
15442|Poolowanna Formation|24372|6|Mentioned|p21|||Geological Province: Cooper Basin.||||||
15442|Poolowanna Formation|24482|5|Briefly described|p44|||Geological Province: Eromanga Basin.||||||
15442|Poolowanna Formation|37776|6|Mentioned|Fig.2|||||||||
15442|Poolowanna Formation|40670|6|Mentioned|Fig.9|||||||||
15442|Poolowanna Formation|40926|6|Mentioned|Table 2|||||||||
15442|Poolowanna Formation|41060|6|Mentioned|p2|||See also Fig.5||||||
15442|Poolowanna Formation|41061|6|Mentioned|p20|||||||||
15442|Poolowanna Formation|41063|2|Defined|p46|Middle Jurassic|Early Jurassic|||||||
15442|Poolowanna Formation|41084|5|Briefly described|Fig.2|||||||||
15442|Poolowanna Formation|41175|6|Mentioned|Fig.1|||||||||
15442|Poolowanna Formation|41176|6|Mentioned|Table 2|||||||||
15442|Poolowanna Formation|41183|6|Mentioned|p310|||||||||
15442|Poolowanna Formation|41187|6|Mentioned|Fig.2|||||||||
15442|Poolowanna Formation|41216|6|Mentioned|p300|||||||||
15442|Poolowanna Formation|41724|6|Mentioned|p381|||||||||
15442|Poolowanna Formation|42008|5|Briefly described|p266|||||||||
15442|Poolowanna Formation|42357|6|Mentioned|p11|||||||||
15442|Poolowanna Formation|42463|6|Mentioned|Fig.4 P171|||||||||
15442|Poolowanna Formation|42520|5|Briefly described|p6|||||||||
15442|Poolowanna Formation|42746|4|Described|p10|||See also Fig.6.||||||17-JAN-08
15442|Poolowanna Formation|43052|5|Briefly described|Table 2.1|||||||||
15442|Poolowanna Formation|43628|6|Mentioned|Fig.3|Early Jurassic|Early Jurassic|||||||
15442|Poolowanna Formation|44133|4|Described|p105|Jurassic|Early Jurassic|Previously known as 'Cuttapirie beds', 'basal Hutton', and 'basal Jurassic'. Maximum Thickness in type section 206m. Intertongues with and is overlain by the Algebuckina Sandstone and Hutton Sandstone.||||||17-JAN-08
15442|Poolowanna Formation|60386|6|Mentioned|p299|Early Jurassic|Early Jurassic|Cooper/Eromanga Basin. Non-marine.||||||
15442|Poolowanna Formation|60717|5|Briefly described|p40 Fig. 2, p42|Middle Jurassic|Early Jurassic|Unconformity at base, over the Cuddapan Formation. Overlain by Hutton Sandstone. Geological Province: Eromanga Basin.||||||31-JAN-08
15442|Poolowanna Formation|61015|6|Mentioned|p44, p45|Early Jurassic|Early Jurassic|||||||19-APR-05
15442|Poolowanna Formation|61613|6|Mentioned|p282 Fig. 2|Middle Jurassic|Early Jurassic|Geological Province: Eromanga Basin.||||||07-FEB-11
15442|Poolowanna Formation|61614|6|Mentioned|p289, p297, p290 Fig. 2|Early Jurassic|Early Jurassic|Geological Province: Eromanga Basin. Contain coals and shales.||||||17-MAR-09
15442|Poolowanna Formation|61615|5|Briefly described|p302, p302 Fig. 2, p305, p306, p307|Middle Jurassic|Jurassic|Geological Province: Eromanga Basin. Comprises fluvial sandstones interbedded with shales and discontinuous, thin coals.||||||09-MAY-13
15442|Poolowanna Formation|62046|5|Briefly described|p125 Fig. 2|Jurassic|Jurassic|Geological Province: Cooper-Eromanga Basins.||||||14-APR-08
15442|Poolowanna Formation|62376|5|Briefly described|p84|Middle Jurassic|Late Triassic|Geological Province: Pedirka Basin.||||||09-FEB-10
15442|Poolowanna Formation|62537|6|Mentioned|p191 Fig.2, p192.|Middle Jurassic|Early Jurassic|Eromanga Basin. Significant hydrocarbon source potential.||||Is overlain by Hutton and Algebuckina Sandstones.||
15442|Poolowanna Formation|62730|5|Briefly described|p352 Fig. 1|Early Jurassic|Early Jurassic|Geological Province: Eromanga Basin.||||||14-APR-08
15442|Poolowanna Formation|63979|2|Defined|p32, Fig. 44|Toarcian|Pleinsbachian|Supersedes "Poolowanna beds". Unconformable on Cuddapan Fm; conformable below Hutton Sandstone. Max.thick: 165m.Comprises lower dominantly sandstone subunit + upper dominantly mudstone subunit - more lithology available.Geol. Prov.Eromanga Basin.||||||07-FEB-11
15442|Poolowanna Formation|64048|5|Briefly described|p64 Tb. 2, p69|||Geological Province: Eromanga Basin. Possesses hydrocarbon source potential.||||||07-FEB-11
15442|Poolowanna Formation|64197|6|Mentioned|p625 Fig.1c|Early Jurassic|Early Jurassic|Overlies the Nappamerri Unconformity.||||Underlies the Hutton Sandstone.||
15442|Poolowanna Formation|64232|5|Briefly described|p12|Jurassic|Jurassic|Geological Province: Eromanga Basin. Coal occurs in deeper parts of the basin in this unit.||||||24-JUL-08
15442|Poolowanna Formation|64665|5|Briefly described|p53 Fig.2, p61.|Early Jurassic|Early Jurassic|Eromanga Basin. Lateral equivalent of Precipice Sandstone and Evergreen Formation in the Surat Basin. Hosts thin (to 0.5 m thick) uneconomic coal seams.||||Is overlain by Hutton Sandstone.||
15442|Poolowanna Formation|64778|6|Mentioned|p13, 21, 28|Jurassic|Jurassic|Pedirka and Simpson Desert Basins. Appears as Poolawanna Formation on p13.  Potential hydrocarbon source.||||Is overlain by Algebuckina Formation.||
15442|Poolowanna Formation|65238|5|Briefly described|p3, p7 Fig. 8|Jurassic|Jurassic|Overlies Purni Formation. Geological province: Eromanga Basin. Meandering and anastomosing fluvial-floodplain deposits. See also p10, p14 Fig. 17.||||||16-FEB-10
15442|Poolowanna Formation|65385|5|Briefly described|pS134 Fig.7|Early Jurassic|Early Jurassic|Of Eromanga Basin. Overlain by Hutton Sandstone.||||||08-MAR-12
15442|Poolowanna Formation|65489|5|Briefly described|p15, p24, p26, p45, p47,p49, p53, p55-62|Early Jurassic|Early Jurassic|See also p91, p96, p137, p151-152, p154-160. Eromanga Basin. 130-290m thick. Hydrocarbon source rock. Stratigraphic and structural trapping of Permian generated oil. Gas and oil reservoir accounting for 6.3% and 5% respectively of the Basin's production. Intraformational shale seal.||||Overlies Cuddapan Formation unconformably. Is overlain by Algebuckina Sandstone.|Includes meandering fluvial sandstones and organic-rich shales.|
15442|Poolowanna Formation|65925|5|Briefly described|Appendix 2.||||||||White to pale grey, fine- to medium-grained, crossbedded sandstone, ripple cross laminated; dark grey siltstone; shale; coal seams and breccias.|
15442|Poolowanna Formation|66529|6|Mentioned|p12 Fig.5|||Eromanga Basin.||||Unconformably overlies Nappamerri Group. Is overlain by Algebuckina Sandstone and Hutton Sandstone.||
15442|Poolowanna Formation|66915|5|Briefly described|p6 Fig.3|Early Jurassic|Early Jurassic|Eromanga Basin.||||||
15442|Poolowanna Formation|67323|5|Briefly described|p87-88, p95 Fig.12.5|Early Jurassic|Early Jurassic|Eromanga/Galilee Basins. Hydrocarbon exploration target in the Eromanga Basin.||||Is overlain by Hutton Sandstone.||
15442|Poolowanna Formation|67402|6|Mentioned|p114 fig ERO13, p117|||Seel also the Poolowanna Formation, Lower and Poolowanna Formation, Upper.||||||
15442|Poolowanna Formation|68731|6|Mentioned|p208, pp209-211|Jurassic|Jurassic|See also Poolawanna Formation.||||Unconformably overlies Tinchoo Formation (Nappamerri Group).||17-JUL-14
15442|Poolowanna Formation|69001|6|Mentioned|p16|Early Cretaceous|Jurassic|Recent interpretations by the NSW DPI broadly group this unit within the Algebuckina Sandstone and equivalent units.||||||
15442|Poolowanna Formation|69019|5|Briefly described|p85 Fig.21.|Early Jurassic|Early Jurassic|Southern Eromanga Basin.||||Is overlain by Algebuckina and Hutton Sandstones.||
15442|Poolowanna Formation|69023|6|Mentioned|p86, p89 Fig.20, p90|Middle Jurassic|Early Jurassic|||||||
15442|Poolowanna Formation|69454|5|Briefly described|p38:3, 7 Fig.38.6; 38:12-13, 14 Fig.38.9|Early Jurassic|Early Jurassic|Eromanga Basin. Sandstones have fair to good reservoir potential, sealed by intra-formational shales.||||Unconformably overlies Peera Peera Formation. Is overlain by Algebuckina Sandstone.||12-JUL-16
15442|Poolowanna Formation|69457|4|Described|p41:2-4; 41:5 Fig.41.4; 41:15-17|Early Jurassic|Early Jurassic|Moore (1986); formerly Poolowanna beds of Wiltshire (1978). Eromanga Basin; entirely subsurface. 205m thick; thins to the W. Fluvial and lacustrine deposits. Pliensbachian-Toarcian age. The coal is black, dull and shaly and the thin (0.5m thick) seams are uneconomic. Contains confirmed oil source rocks with TOCs up to 15%. Thermal maturity, prospects and leads discussed in some detail. Lacustrine shales might form a regional seal. Contains the deepest reservoir units in the Eromanga Basin succession.||||Unconformably overlies Cuddapan Formation. Is overlain conformably by/intertongues with Hutton Sandstone and Algebuckina Sandstone. Lateral equivalent of Precipice Sandstone and Evergreen Formation.|Sandstone, siltstone and coaly shale, arranged in two upward-fining cycles. Thin discontinuous coal seams.|12-JUL-16
15442|Poolowanna Formation|69582|6|Mentioned|p65|Early Jurassic|Early Jurassic|Eromanga Basin.||||Overlain by the Hutton Sandstone.||
15442|Poolowanna Formation|69594|4|Described|p519, p524, p526, p531-532, p535, p545|Early Jurassic|Early Jurassic|See also p572. Eromanga Basin. Originally defined in the Poolowanna Trough in SA (Wiltshire, 1978; Moore, 1986); the type section is in DIO Poolowanna 1. Maximum thickness is 165m. Represents cyclic fluvio-lacustrine deposition. Palynofloras in QLD are Pliensbachian-Toarcian and are generally correlated with those of upper Precipice Sandstone-Evergreen Formation. Is a minor hydrocarbon reservoir; has hydrocarbon source potential. RELATED UNITS (continued): Passes laterally into Precipice Sandstone. Equivalent to Evergreen Formation.||||Unconformably overlies Cuddapan, Tinchoo, Toolachee and Patchawarra Formations. Is overlain conformably by Hutton Sandstone (and intertongues with it) and Algebuckina Sandstone. See COMMENTS for more.||
15442|Poolowanna Formation|69633|6|Mentioned|p14|||Eromanga Basin.||||||
15442|Poolowanna Formation|69673|5|Briefly described|p154, p154 fig 126, p159, p160, p161|Jurassic|Jurassic|Up to 205m thick. Confirmed oil source rock.||||Unconformably (or disconformably) overlain by Algebuckina Sandstone, Hutton Sandstone, overlies Walkandi Formation, unconformably overlies Peera Peera Formation|Interbedded sandstone that fines upwards into coaly shale and siltstone.|
15442|Poolowanna Formation|69790|6|Mentioned|p1063 Fig.2|Early Jurassic|Early Jurassic|Eromanga Basin.||||||
15442|Poolowanna Formation|69797|5|Briefly described|p17 incl Fig.2|Middle Jurassic|Early Jurassic|The best petroleum source rocks in Jurassic-Cretaceous sequence of Eromanga Basin are the highly carbonaceous shales of Poolowanna Formation, the coals and carbonaceous shales of Birkhead Formation, and organic-rich shales and siltstones of Murta Formation. Age approximated from figure. Geol. Prov: Eromanga Basin.||||||17-JAN-17
15442|Poolowanna Formation|69946|3|Fully described|p10-11, p51, p57-60, p74-82|Middle Jurassic|Early Jurassic|Eromanga Basin. Moore (1986); formerly Poolowanna beds (Wiltshire, 1978). Type section remains that of Wiltshire (1978), viz. the interval 2387 - 2593m in Poolowanna 1; not the interval 2422-2476m in Cuttapirrie 1 which has also been called Poolowanna Formation and 'Cuttapirrie beds' in SA. Up to 205m thick. Wireline log correlations.||||Intertongues with, and is overlain by, Algebuckina and Hutton Sandstones.|Interbedded grey to brown carbonaceous siltstone; pale grey to buff, very fine- to medium-grained sandstone; rare coal seams.|
15442|Poolowanna Formation|69947|5|Briefly described|p3-5, p13 Fig.7.2, p16-21 Figs.7.5-10|Early Jurassic|Early Jurassic|See also p23 Fig.7.12. Eromanga Basin. First deposits above the basal Eromanga Basin unconformity. Amalgamated channel sands and infilled palaeovalleys; no laterally extensive sand sheets. Facies described in some detail.||||Unconformably overlies Cuddapan Formation. Is overlain by Hutton Sandstone.|Sandstone, minor shale and thin coal seams.|
15442|Poolowanna Formation|69948|6|Mentioned|Fig.4.18|||Eromanga Basin.||||Unconformably overlies Peera Peera and Purni Formations. Is overlain by Algebuckina Sandstone.||
15442|Poolowanna Formation|69982|6|Mentioned|p49-50|Early Jurassic|Early Jurassic|The Sturt 7 oil well was re-perforated in this unit after extracting Mooracoochie Volcanics oil, extending production by almost one-half.||||||
15442|Poolowanna Formation|70823|4|Described|p25-p27, p43-p44, p78|Early Jurassic|Early Jurassic|Eromanga Basin. Deposited in a meandering-anastomosing fluvial or lacustrine or overbank environments. Up to 130m thick. This unit forms a source rock that hosts an oil and gas discovery.||||Unconformably overlies the Cuddapan Formation. Overlain by the Hutton Sandstone.|Sandstone, siltstone, shale and coal.|
15442|Poolowanna Formation|70824|5|Briefly described|p9|Jurassic|Jurassic|Eromanga Basin.||||Overlies the Cuddapan Formation. Overlain by the Hutton Sandstone.||
15442|Poolowanna Formation|71321|6|Mentioned|p15|||Of Eromanga Basin.||||Overlies the Peera Peera Formation. Overlain by the Algebuckina Sandstone.||24-OCT-19
15442|Poolowanna Formation|71342|3|Fully described|Ch 1 p3, Ch4 p25,  Ch5 p10-p12, Ch5 p30|Aalenian|Hettangian|Eromanga Basin. Source of significant production of gas in the Eromanga Basin. Originally the Poolowanna beds of Wiltshire (1978) before being raised to formation status by Moore (1986). This unit has also been previously referred to as the 'basal Hutton Sandstone', 'Cuttapirrie beds' (in South Australia or as the 'basal Jurassic' (in Queensland). A type section is mentioned in Poolowanna 1. Petrography is discussed in some detail. Spore-pollen zone is given in Ch5 p57. Reaches a maximum thickness of 205m in Poolowanna 1. Interpreted to have been deposited in fluvial channels meandering across a floodplain with minor coal swamps. Sequence stratigraphy discussed in detail (Ch7) as is source rock potential and hydrocarbon geochemistry (Ch8). See also Ch5 p51, Ch5 p57-p59, Ch5 p74, Ch6 p5-p6, Ch7 p3-p5, Ch7 p10, Ch7 p13, Ch7 p16-p17, Ch7 p20, Ch8 p2, Ch8 p8, Ch8 p10-p11, Ch9 p5, Ch9 p11, Ch9 p18, Ch10 p3, Ch10 tbl 10.1, Ch10 p6, Ch10 p14, Ch10 p17, Ch11 p2, Ch11 p7-p8, Ch11 p13, Ch12 p2p3, Ch12 tbl 12.1, Ch12 p6, Ch12 p9, Ch12 p11-p14, Ch13 p3, Ch13 p8, Ch14 p2-p7.||||Unconformably overlies the Peera Peera and Cuddapan Formations. Overlain by the Algebuckina and Hutton sandstones.|Interbedded carbonaceous siltstone, sandstone and rare coal seams. Sandstones range from very fine to medium grained and contain minor pebbles and granules of quartzite and reworked basement.|
15442|Poolowanna Formation|71805|5|Briefly described|p75-p76|Toarcian|Pleinsbachian|Eromanga Basin. This unit is temporally equivalent to the Precipice Sandstone.||||Overlain by the Hutton Sandstone.||16-MAY-19
15442|Poolowanna Formation|71863|5|Briefly described|p4|||Eromanga Basin. Potential petroleum source (although the majority is derived from the underlying Cooper Basin units).||||||
15442|Poolowanna Formation|72297|5|Briefly described|p739, p742-743|||Eromanga Basin. Petroleum reservoir, with source rock potential.||||||
15442|Poolowanna Formation|72298|5|Briefly described|p801|Jurassic|Jurassic|Eromanga Basin (SA,QLD).||||Unconformably overlies Nappamerri Group. Is overlain by Algebuckina, Hutton Sandstones.||
15442|Poolowanna Formation|72476|6|Mentioned|p36 Fig.9, p37|||Eromanga Basin. Time-temperature thermal history diagram. Only <1 km thickness preserved.||||||
15442|Poolowanna Formation|73167|6|Mentioned|p664 Fig. 2|Jurassic|Jurassic|Eromanga Basin. Contains oil.||||||
15442|Poolowanna Formation|73249|6|Mentioned|p319|Cretaceous|Jurassic|Eromanga Basin.||||||
15442|Poolowanna Formation|73251|6|Mentioned|p49, p55-56, p62|Early Jurassic|Early Jurassic|Eromanga Basin. Meandering-anastomosing fluvial depositional setting. Hydrocarbon source rock that contains[?] gas and oil.||||Overlain by Hutton Sandstone.||
15442|Poolowanna Formation|73281|6|Mentioned|p1, Appendix (DIP)|Early Jurassic|Early Jurassic|Eromanga Basin. Petroleum source rocks. See DIP034_Petroleumdata.xlsx and DIP034_Welldata.xlsx. Also written as Poolowanna Formation, lower.||||||
15442|Poolowanna Formation|73343|6|Mentioned|p337|Jurassic|Jurassic|Eromanga Basin. Hosts oil.||||Overlain by Hutton Sandstone.||
15442|Poolowanna Formation|73479|5|Briefly described|p156 Fig.2, p159, p179|Jurassic|Jurassic|Eromanga Basin. Fluvial depositional environment.|ca 200-180 Ma|||Unconformably overlies Cuddapan Formation, underlies Hutton Sandstone||
15448|Pooraka Formation|10010|6|Mentioned|p14 Fig. 5e|||Geological Province: Murray Basin. Reworked colluvial outwash fans material.||||||13-AUG-07
15448|Pooraka Formation|22887|3|Fully described|p50|Late Pleistocene|Late Pleistocene|||||||
15448|Pooraka Formation|23054|6|Mentioned|p30|||||||||
15448|Pooraka Formation|23252|5|Briefly described|Map Legend||Pleistocene|||||||
15448|Pooraka Formation|23489|5|Briefly described|p43 Table 1|Pleistocene|Pleistocene|||||||
15448|Pooraka Formation|23719|4|Described|p29|Late Pleistocene|Late Pleistocene|See also page 30 table 9. Overlying unit Wiabuna Formation. Underlying unit Gibbon Beds. Max. thickness 5 m.||||||14-NOV-13
15448|Pooraka Formation|23818|4|Described|p212 Fig.108, p224|Late Pleistocene|Late Pleistocene|Geological Province: St. Vincent Basin. Overlying unit: Saint Kilda Formation. Underlying units: Hindmarsh Clay and Ripon Calcrete. Max. thickness: 20 ft.||||||18-APR-05
15448|Pooraka Formation|23887|6|Mentioned|p205|||||||||
15448|Pooraka Formation|24176|5|Briefly described|p21, p22 Tb. 1|Late Pleistocene|Late Pleistocene|Reddish clay-sand with lime horizon (Loveday Soil) near top.  Geological Province: Mount Painter Province.||||||
15448|Pooraka Formation|24484|5|Briefly described|p805|Quaternary|Quaternary|Max. Thickness: 10m.||||||
15448|Pooraka Formation|24566|5|Briefly described|p111, p114 Fig. 8|||Includes the Wilkatana fanglomerates.  Boulder conglomerates. Overlies Port Willunga Formation. Age: ca130-120Ka.||||||
15448|Pooraka Formation|29697|5|Briefly described|Table 3|||||||||
15448|Pooraka Formation|30055|6|Mentioned|p152|||||||||
15448|Pooraka Formation|30056|6|Mentioned|p148|||||||||
15448|Pooraka Formation|30176|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
15448|Pooraka Formation|30750|6|Mentioned|p3|||Upper Pleistocene age.||||||
15448|Pooraka Formation|30753|6|Mentioned|p15|||||||||
15448|Pooraka Formation|30754|4|Described|p35|||Stratigraphic table p22.||||||09-SEP-22
15448|Pooraka Formation|30756|6|Mentioned|p4|||||||||
15448|Pooraka Formation|30757|6|Mentioned|p2|||||||||
15448|Pooraka Formation|30758|6|Mentioned|p67|||Important source of fine aggregate & clay, P69||||||
15448|Pooraka Formation|30802|6|Mentioned|p10|||Pleistocene age||||||
15448|Pooraka Formation|30807|6|Mentioned|p101|||Suggested map symbol||||||
15448|Pooraka Formation|30924|6|Mentioned|Map legend|Recent|Pleistocene|Pleistocene - Recent||||||
15448|Pooraka Formation|31895|4|Described|p411|||Radiocarbon age||||||
15448|Pooraka Formation|31921|6|Mentioned|p6|||See also Fig.3||||||
15448|Pooraka Formation|31966|6|Mentioned|p6|||Equivalent mentioned||||||
15448|Pooraka Formation|32432|6|Mentioned|Fig.2|||See also Table 1||||||
15448|Pooraka Formation|32547|4|Described|p60|||Quaternary||||||
15448|Pooraka Formation|33422|6|Mentioned|Map legend|Cenozoic|Cenozoic|||||||19-NOV-08
15448|Pooraka Formation|33423|6|Mentioned|p14|||Strat.||||||
15448|Pooraka Formation|33557|6|Mentioned|Fig.2|||Map of Gawler Range Volcanic Complex||||||
15448|Pooraka Formation|33834|6|Mentioned|p16|||||||||
15448|Pooraka Formation|34069|6|Mentioned|Fig.3|||||||||
15448|Pooraka Formation|34180|5|Briefly described|p224|||See also P212||||||
15448|Pooraka Formation|34181|4|Described|p46|||See also pp57,53. Pleistocene||||||22-DEC-21
15448|Pooraka Formation|34536|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
15448|Pooraka Formation|34758|6|Mentioned|Table 1|||||||||
15448|Pooraka Formation|35097|6|Mentioned|Fig.4|||||||||
15448|Pooraka Formation|35159|5|Briefly described|p12|||See also Fig.2.||||||
15448|Pooraka Formation|35200|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
15448|Pooraka Formation|35232|5|Briefly described|Table.4|||||||||
15448|Pooraka Formation|35673|6|Mentioned|Fig.1|||Location plan, Para Hills quartzite quarry.||||||
15448|Pooraka Formation|35772|6|Mentioned|p13|||||||||
15448|Pooraka Formation|35905|6|Mentioned|p2|||||||||
15448|Pooraka Formation|36621|6|Mentioned|Fig.1|||||||||
15448|Pooraka Formation|36626|6|Mentioned|Fig.1|||||||||
15448|Pooraka Formation|36834|6|Mentioned|Fig.1|||||||||
15448|Pooraka Formation|36835|6|Mentioned|Fig.1|||||||||
15448|Pooraka Formation|37853|6|Mentioned|Fig.1|||||||||
15448|Pooraka Formation|38068|5|Briefly described|p76|||See also P77.||||||
15448|Pooraka Formation|38107|6|Mentioned|Fig.2|||||||||
15448|Pooraka Formation|38605|6|Mentioned|p40|||||||||
15448|Pooraka Formation|39349|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
15448|Pooraka Formation|39351|6|Mentioned|Map legend|Quaternary|Quaternary|||||||
15448|Pooraka Formation|39352|6|Mentioned|Map legend|late Holocene|Pleistocene|Pleistocene to Holocene||||||
15448|Pooraka Formation|40003|5|Briefly described|Table 4|||||||||
15448|Pooraka Formation|40149|6|Mentioned|p122|||||||||
15448|Pooraka Formation|40219|6|Mentioned|p3|||||||||
15448|Pooraka Formation|40439|6|Mentioned|p382|||||||||
15448|Pooraka Formation|40442|6|Mentioned|p37|||See also Fig.23,||||||
15448|Pooraka Formation|40450|6|Mentioned|p67|||||||||
15448|Pooraka Formation|40502|5|Briefly described|p83|||||||||
15448|Pooraka Formation|40910|6|Mentioned|p19|||||||||
15448|Pooraka Formation|40911|6|Mentioned|Map legend|Quaternary|Quaternary|||||||
15448|Pooraka Formation|40914|6|Mentioned|Map legend|Cenozoic|Cenozoic|||||||19-NOV-08
15448|Pooraka Formation|40926|6|Mentioned|Table 3|||||||||
15448|Pooraka Formation|41119|6|Mentioned|p8|||||||||
15448|Pooraka Formation|41151|6|Mentioned|p14|||||||||
15448|Pooraka Formation|41292|6|Mentioned|Fig.1|||||||||
15448|Pooraka Formation|41362|6|Mentioned|p7|||||||||
15448|Pooraka Formation|41506|5|Briefly described|Fig.2|||||||||
15448|Pooraka Formation|41520|5|Briefly described|Fig.5|||||||||
15448|Pooraka Formation|41619|6|Mentioned|Map legend|Pleistocene||||||||
15448|Pooraka Formation|42457|5|Briefly described|p163|||of Firman (1969)||||||
15448|Pooraka Formation|42466|6|Mentioned|Map legend|||||||||
15448|Pooraka Formation|42469|6|Mentioned|p48|||||||||
15448|Pooraka Formation|42475|6|Mentioned|p24|||||||||
15448|Pooraka Formation|42498|5|Briefly described|Map legend|late Pleistocene|Pleistocene|||||||
15448|Pooraka Formation|42499|5|Briefly described|Map legend|Pleistocene||||||||
15448|Pooraka Formation|42506|5|Briefly described|Map legend|Pleistocene||||||||
15448|Pooraka Formation|42716|5|Briefly described|Map legend|Pleistocene||||||||
15448|Pooraka Formation|42720|5|Briefly described|map legend|Pleistocene||||||||
15448|Pooraka Formation|42721|6|Mentioned|map legend|Holocene||||||||
15448|Pooraka Formation|42722|6|Mentioned|map legend|Pleistocene|Pleistocene|Presented as an equivalent of this formation.||||||07-APR-05
15448|Pooraka Formation|42733|5|Briefly described|map legend|Quaternary||||||||
15448|Pooraka Formation|42738|5|Briefly described|map legend|Quaternary||||||||
15448|Pooraka Formation|42813|6|Mentioned|p25|||||||||
15448|Pooraka Formation|42966|2|Defined|p211|Late Pleistocene||||||||
15448|Pooraka Formation|43049|5|Briefly described|p27|||||||||
15448|Pooraka Formation|43053|5|Briefly described|Map Legend|Pleistocene|Pleistocene|||||||25-MAY-05
15448|Pooraka Formation|43071|5|Briefly described|p17,Table 3|||||||||
15448|Pooraka Formation|43094|6|Mentioned|p40|||||||||
15448|Pooraka Formation|43258|5|Briefly described|Map Legend|Holocene|Pleistocene|||||||
15448|Pooraka Formation|43298|6|Mentioned|Map Legend|Holocene|Pleistocene|||||||
15448|Pooraka Formation|44133|4|Described|p220 Fig. 11.2, 242|Late Pleistocene|Late Pleistocene|Age: ~35,000 BP (Williams 1937b), 30,000-20,000 BP (Belperio and Bateman 1986). Thickness: 450m. Geological Province: Saint Vincent Basin?.||||||22-DEC-21
15448|Pooraka Formation|44188|5|Briefly described|Map Legend|Holocene|Pleistocene|Geological province: Murray Basin. Unconsolidated, red-brown, poorly sorted clayey sand, gravel, conglomerate, breccia; local calcrete intercalations and cappings; in places cemented by ferruginised silicified matrix.||||||15-MAY-08
15448|Pooraka Formation|44660|14|Not recorded|map legend||Pleistocene|Pleistocene, lithology.||||||
15448|Pooraka Formation|49038|4|Described|Table 2|||Briefly described P33||||||
15448|Pooraka Formation|60953|5|Briefly described|Map Legend|Pleistocene|Pleistocene|Gravelly and sandy clay, commonly gypcreted or calcreted.||||||
15448|Pooraka Formation|61070|5|Briefly described|Map Legend|Late Pleistocene|Middle Pleistocene|Alluvial reddish brown and yellowish brown gravelly and sandy clay, silt and sand with soft earthy carbonate.||||||12-JAN-10
15448|Pooraka Formation|61108|5|Briefly described|map legend|Pleistocene|Pleistocene|Gravelly and sandy clay of piedmont slopes and alluvial plains, commonly gypcreted or calcreted.||||||
15448|Pooraka Formation|61964|6|Mentioned|p175, p190|||Geological Province: Murray Basin. See also p192.||||||
15448|Pooraka Formation|62096|5|Briefly described|p288|||Variously referred to as Pooraka Formation I, P.F. !! and P.F. III, as well as various versions of Pooraka Formation gravels - see Pooraka Formation gravels for variations.||||||09-MAY-06
15448|Pooraka Formation|62577|6|Mentioned|p566|Late Pleistocene|Late Pleistocene|Mentioned only in the context of 'Pooraka Formation equivalents' in relation to Germein Bay Formation.  Alluvial deposits||||||
15448|Pooraka Formation|62893|4|Described|Map Legend, p24|Holocene|Pleistocene|Colluvial and fluvial. Forms veneers over locally exposed calcrete. Best developed as an apron around the Cleve Uplands and around granitic inselnergs to the northwest.|||||Dark brown and mottled green gravelly clay, silt, clay and conglomerate.|
15448|Pooraka Formation|64705|5|Briefly described|p80 Fig. 7d (photo)|Quaternary|Quaternary|Age: <120,000a. Sediments.||||||04-DEC-08
15448|Pooraka Formation|65552|6|Mentioned|p6, p27 App.6|Late Pleistocene|Late Pleistocene|Murray Basin unit. Derived from eastern flanks of Mount Lofty Ranges and Flinders Ranges. Hosts some silica sands resources. Mixed aeolian and colluvial deposits or outwash fans comparable with deposits along the margins of the Riverine Plain in NSW.||||||
15448|Pooraka Formation|65901|4|Described|p175-81, p181 Fig.4, p183-6, p183 Fig.5|Pleistocene|Pleistocene|Also called Hookina Creek Formation by Williams (1982). Fluvial. Optically stimulated luminescence age. Younger alluvial sediments, ages ~ 71 - 29 ka (Quigley et al. 2007) are no longer considered part of Pooraka Formation.|132-118 ka (Chen 1991).|||Overlies Taringa Formation. Interfingers with Glanville Formation.|Red/brown sandy clay deposit with occasional gravel lenses.|08-MAR-12
15448|Pooraka Formation|65922|5|Briefly described|p25 Tb. 4, p27|Pleistocene|Pleistocene|Red-brown-yellowish brown gravelly to sandy clay, silt and sand; local soft carbonate. Fluvial surface unit developed around the flanks and within the Gawler Ranges. Small-scale quarrying for aggregate.||||||
15448|Pooraka Formation|68068|5|Briefly described|Map legend|Pleistocene|Pleistocene|Callabonna Sub-basin, Lake Eyre Basin. An equivalent unit is mapped and described. Forms remnant deposits on the upper parts of dissected surfaces and plateaus. Represents a piedmont slope distal deposit.|||||Clay, silt and gravel with minor cobbles; dark yellow to orange to red-brown; upper parts usually fine-grained (silty or clayey) and not gibber clad.|
15448|Pooraka Formation|68126|6|Mentioned|p31|Paleozoic|Paleozoic|||||||
15448|Pooraka Formation|68131|6|Mentioned|p57, p89|Pleistocene|Pleistocene|||||||
15448|Pooraka Formation|68203|5|Briefly described|p9 Fig.6|||Mount Lofty Ranges.|85 +/- 11 ka.|||Overlies and is faulted against Apilla Tillite. Is faulted against Emeroo Quartzite.|Talus breccia overlain by river gravels.|
15448|Pooraka Formation|69019|5|Briefly described|p106 Fig.26, p122.|Pliocene|Pliocene|Of Firman (1966). W of Lake Blanche. Represents a distal piedmont slope deposit. Thickness from <1 to >3 m. Widely varying ages listed.|||||Dark yellow to red-brown clay, silt and gravel with minor cobbles forming remnant deposits on the upper parts of dissected surfaces and plateaus; much lateral facies change.|
15448|Pooraka Formation|69023|5|Briefly described|p128|Holocene|Pleistocene|Defined by Firman (1966); named after the Adelaide suburb of Pooraka. Found to be widespread as sedimentary aprons around the Mount Lofty and Flinders Ranges. Forms remnant deposits on the upper parts of dissected surfaces and plateaus. Variable thickness: <1 to ~3m.||||Unconformably overlies Bulldog Shale.|Clay, silt and gravel with minor cobbles; dark yellow to red-brown; lower parts more clay-rich; well-developed calcareous soil horizons with earthy to pisolitic carbonate or gypsum segregations are common in basal parts.|
15448|Pooraka Formation|69649|5|Briefly described|p33|||Forms an apron of variable thickness over much of eastern CHILDARA.|||||Alluvial, reddish-brown, sandy clay.|
15448|Pooraka Formation|69666|6|Mentioned|p25|||||||||
15448|Pooraka Formation|70333|5|Briefly described|Map legend.|Pleistocene|Pleistocene||||||Clay, sand and carbonate earth, silty, with gravel lenses.|
15448|Pooraka Formation|70334|6|Mentioned|p62,65-66|||Alluvial sediments which underlie the Adelaide Plains.||||||
15448|Pooraka Formation|70384|5|Briefly described|Map legend.|Pleistocene|Pleistocene|Piedmont slope distal deposit. Remnants on dissected surfaces and plateaus. Relict 1-5m thick sheets of the lower, gravelly part emerge from rangelands and some intertongue distally with the upper silty/clayey part.|||||Clay, silt, gravel, minor cobbles; dark yellow to orange to red-brown. Upper part mostly silty or clayey, not gibber-clad. High terrace gravels: fluvial, cobble to gravel, well-rounded polymict clasts, coarse sand matrix. Weakly-moderately cemented.|
15448|Pooraka Formation|70660|5|Briefly described|p30, p32|||An alternative name for the Christies Beach Formation.||||||
15448|Pooraka Formation|71129|6|Mentioned|p166|||Of Adelaide Geosyncline.||||||
15448|Pooraka Formation|71317|5|Briefly described|p144|||The sand plains over Pletabinna were previously mapped as Pooraka Formation, however due to the lack of temporal correlation with these sediments and the Pooraka Formation this was not repeated in this study.|||||Clay, sand and carbonate earth, silty with gravel lenses.|
15448|Pooraka Formation|72456|5|Briefly described|Map Legend|Pleistocene|Pleistocene|Marree 1:250k map sheet.|||||Clay, sand and carbonate earth, salty, with gravel lenses.|
15448|Pooraka Formation|72458|6|Mentioned|p4|Quaternary|Pliocene|||||Underlain by Namba Formation.|Gravels and fanglomerates.|
15448|Pooraka Formation|73103|5|Briefly described|Map legend.|Pleistocene|Pleistocene||||||Clay, sand and carbonate earth, silty, with gravel lenses.|
15448|Pooraka Formation|73110|5|Briefly described|Map legend.|Pleistocene|Pleistocene||||||Clay, sand and carbonate earth, silty, with gravel lenses.|
15448|Pooraka Formation|73188|5|Briefly described|[See comments]|Late Pleistocene|Late Pleistocene|St Vincent Basin. Geochron is thermoluminescence dating; see Bourman et al. (1997). Interpreted as distal sediments sourced from erosion of the rising Mount Lofty Ranges. Records the last significant uplift on a number of Adelaide's faults. p: 319-320, 323-324, 329, 331, 334-335, 337-338, 345-346, 349, 351, 358-359.|ca 0.125 Ma|||Equivalent to Christies Beach Formation.|Alluvial fans, clay, sand, gravel, and wind-blown sand; lacking ferruginous and siliceous induration.|
15448|Pooraka Formation|73228|6|Mentioned|p51|||||||||
15448|Pooraka Formation|73236|4|Described|p36, p38 p43, p46, p48|Late Pleistocene|Late Pleistocene|Alluvial and slope sediments. Forms prominent alluvial fans along the Eden-Burnside and Para fault scarps. Represented at Hallett Cove only by local channel fills of sandy and pebbly clay with rubbly, nodular calcrete paleosols in the north of the map area.|c. 0.13-0.08 Ma|||Underlain by Keswick Clay. Overlain by Ngankipari Sand.|Red-brown clay, locally pebbly and/or sandy, with incipient calcrete nodules.|
15457|Port Augusta Kimberlite|40811|4|Described|p319|||||||||
15457|Port Augusta Kimberlite|71129|6|Mentioned|p136|Early Jurassic|Early Jurassic|||||||
15462|Port Campbell Limestone|22674|5|Briefly described|Fig.2 p719|Late Miocene|Middle Miocene|||||||
15462|Port Campbell Limestone|22875|5|Briefly described|p69|Late Miocene|Middle Miocene|Of the Heytesbury Group.||||||07-MAR-07
15462|Port Campbell Limestone|22944|5|Briefly described|Fig3|||||||||
15462|Port Campbell Limestone|23228|6|Mentioned|Fig2-6p14||Miocene|||||||
15462|Port Campbell Limestone|23230|4|Described|Table4-1p40, Fig4-3p46|Miocene|Miocene|||||||
15462|Port Campbell Limestone|23238|6|Mentioned|p106|||||||||
15462|Port Campbell Limestone|23307|5|Briefly described|Map Legend|Miocene|Miocene|||||||
15462|Port Campbell Limestone|23322|5|Briefly described|957 Fig.2|Miocene|Miocene|Of the Heytesbury Group.  Geological Province: Otway Basin.||||||07-SEP-09
15462|Port Campbell Limestone|23768|5|Briefly described|p28 Fig. 5, p30 Fig.6|||Contains Rutledge Creek Member.  Geological Province: Otway Basin. See also p131 and p162.||||||30-MAR-05
15462|Port Campbell Limestone|23909|5|Briefly described|p291|Miocene|Miocene|Geological Province: Otway Basin.  See also p290 Fig. 3.||||||
15462|Port Campbell Limestone|24056|5|Briefly described|p84 Fig. 2|Pliocene|Miocene|Of Heytesbury Group.  Geological Basin: Otway Basin.||||||
15462|Port Campbell Limestone|24551|5|Briefly described|p292 Fig. 10.3, p732 Table 17.2|||Max thickness: 250m.||||||
15462|Port Campbell Limestone|24562|5|Briefly described|p8 Fig. 2|Miocene|Miocene|Of the Heytesbury Group.  Geological Province: Otway Basin.||||||
15462|Port Campbell Limestone|29425|6|Mentioned|p103|||||||||
15462|Port Campbell Limestone|29591|6|Mentioned|p98|||||||||
15462|Port Campbell Limestone|29823|6|Mentioned|p14|||||||||
15462|Port Campbell Limestone|29825|5|Briefly described|p18|||||||||
15462|Port Campbell Limestone|29856|6|Mentioned|p36|||||||||
15462|Port Campbell Limestone|30576|6|Mentioned|Table 2|||||||||
15462|Port Campbell Limestone|30578|5|Briefly described|p12|||||||||
15462|Port Campbell Limestone|30580|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
15462|Port Campbell Limestone|30675|5|Briefly described|p253|||Lithology and radioactivity.||||||07-MAR-07
15462|Port Campbell Limestone|30728|6|Mentioned|p4|||||||||
15462|Port Campbell Limestone|30932|6|Mentioned|Map legend|Miocene|Miocene|Part of Heytesbury Gp. Equivalent Gambier Lst. (in part)||||||
15462|Port Campbell Limestone|31036|1|Redefined|p213|Tertiary|Tertiary|See also Table 9-1. Unit of Heytesbury Group.||||||07-MAR-07
15462|Port Campbell Limestone|31516|6|Mentioned|p49|||||||||
15462|Port Campbell Limestone|31534|6|Mentioned|p363|||See also Table 19-3||||||
15462|Port Campbell Limestone|31583|6|Mentioned|p18|||Section||||||
15462|Port Campbell Limestone|31625|6|Mentioned|Fig. 5.2|||Miocene||||||
15462|Port Campbell Limestone|31922|6|Mentioned|Fig.2|||||||||
15462|Port Campbell Limestone|32102|6|Mentioned|p177|||Miocene||||||
15462|Port Campbell Limestone|32120|6|Mentioned|p280|||Miocene fauna||||||
15462|Port Campbell Limestone|32233|6|Mentioned|p22|||||||||
15462|Port Campbell Limestone|32499|6|Mentioned|p107|||Miocene||||||
15462|Port Campbell Limestone|32601|6|Mentioned|p692|||||||||
15462|Port Campbell Limestone|32852|6|Mentioned|p15|||||||||
15462|Port Campbell Limestone|33135|5|Briefly described|p17|||||||||
15462|Port Campbell Limestone|33136|6|Mentioned|p17|||||||||
15462|Port Campbell Limestone|33155|5|Briefly described|p124|||||||||
15462|Port Campbell Limestone|33807|6|Mentioned|p97|||||||||
15462|Port Campbell Limestone|34360|6|Mentioned|p11|||||||||
15462|Port Campbell Limestone|34832|6|Mentioned|p23|||||||||
15462|Port Campbell Limestone|34954|6|Mentioned|Fig.35|||Analysis Fig.33.||||||
15462|Port Campbell Limestone|34988|6|Mentioned|p292|||||||||
15462|Port Campbell Limestone|34993|6|Mentioned|p300|||||||||
15462|Port Campbell Limestone|35271|6|Mentioned|Fig.2|||||||||
15462|Port Campbell Limestone|35274|6|Mentioned|Table12.18|||||||||
15462|Port Campbell Limestone|35285|5|Briefly described|p414|||||||||
15462|Port Campbell Limestone|35625|6|Mentioned|Fig.1|||||||||
15462|Port Campbell Limestone|35722|6|Mentioned|p4|||Stratigraphy.||||||
15462|Port Campbell Limestone|36119|6|Mentioned|p56|||||||||
15462|Port Campbell Limestone|36913|6|Mentioned|p79|||See also p81.||||||07-MAR-07
15462|Port Campbell Limestone|37583|6|Mentioned|p158|||||||||
15462|Port Campbell Limestone|37585|6|Mentioned|p40|||||||||
15462|Port Campbell Limestone|37587|6|Mentioned|p34|||||||||
15462|Port Campbell Limestone|38150|6|Mentioned|p23|||||||||
15462|Port Campbell Limestone|38625|6|Mentioned|Table 2|||||||||
15462|Port Campbell Limestone|41016|5|Briefly described|Table 1|||||||||
15462|Port Campbell Limestone|41043|6|Mentioned|p97|||||||||
15462|Port Campbell Limestone|41075|6|Mentioned|p18|||||||||
15462|Port Campbell Limestone|41076|6|Mentioned|p59|||||||||
15462|Port Campbell Limestone|41185|6|Mentioned|Fig.4|||||||||
15462|Port Campbell Limestone|41269|6|Mentioned|Fig.2|||||||||
15462|Port Campbell Limestone|41519|6|Mentioned|p168|||||||||
15462|Port Campbell Limestone|41538|6|Mentioned|p304|||||||||
15462|Port Campbell Limestone|41642|6|Mentioned|Fig.8.6|||||||||
15462|Port Campbell Limestone|41701|6|Mentioned|Map legend|Miocene||||||||
15462|Port Campbell Limestone|41704|6|Mentioned|Fig.3|||||||||
15462|Port Campbell Limestone|41714|6|Mentioned|p301|||||||||
15462|Port Campbell Limestone|41726|6|Mentioned|Fig.5|||||||||
15462|Port Campbell Limestone|41769|4|Described|p33|||||||||
15462|Port Campbell Limestone|41848|6|Mentioned|p367|||underlies Bridgewater Formation||||||
15462|Port Campbell Limestone|41868|5|Briefly described|p577|||Mention p548 and Fig.12.30.||||||07-MAR-07
15462|Port Campbell Limestone|42079|6|Mentioned|Fig.2 P264|||See also Fig.10, p272.||||||
15462|Port Campbell Limestone|42318|5|Briefly described|p8|||||||||
15462|Port Campbell Limestone|42473|6|Mentioned|p60|||||||||
15462|Port Campbell Limestone|42524|5|Briefly described|Fig.3 P27|||||||||
15462|Port Campbell Limestone|42635|5|Briefly described|p90|||(Gambier Limestone)||||||
15462|Port Campbell Limestone|42827|3|Fully described|p286|||See also Fig 8.7.||||||07-MAR-07
15462|Port Campbell Limestone|42863|5|Briefly described|Fig.14|||||||||
15462|Port Campbell Limestone|43171|6|Mentioned|5-8|||Of Heytesbury Group. Age: 10-20Ma||||||
15462|Port Campbell Limestone|43208|5|Briefly described|map legend|Late Miocene|Early Miocene|Of Heytesbury Group||||||
15462|Port Campbell Limestone|43219|5|Briefly described|Fig.3,p6.||Miocene|Of Heytesbury Group||||||07-MAR-07
15462|Port Campbell Limestone|43590|4|Described|p26|Late Miocene|Middle Miocene|||||||
15462|Port Campbell Limestone|43604|4|Described|p144|Pliocene|Miocene|||||||
15462|Port Campbell Limestone|43660|6|Mentioned|Fig.6,p15||Oligocene|||||||
15462|Port Campbell Limestone|43667|6|Mentioned|Fig.3,p12|Late Miocene|Middle Miocene|||||||
15462|Port Campbell Limestone|43733|6|Mentioned|Fig.2.11,p65||Miocene|||||||
15462|Port Campbell Limestone|43744|6|Mentioned|Fig.3,p3|||||||||
15462|Port Campbell Limestone|43937|5|Briefly described|Map Legend|Early Oligocene|Middle Eocene|||||||
15462|Port Campbell Limestone|45160|6|Mentioned|p6|||||||||
15462|Port Campbell Limestone|48581|14|Not recorded|p13,14|||||||||
15462|Port Campbell Limestone|48911|6|Mentioned|p27|||See also Chart 1||||||
15462|Port Campbell Limestone|48977|6|Mentioned|Fig.5|||||||||
15462|Port Campbell Limestone|50154|5|Briefly described|p135|||Of Heytesbury Group.||||||
15462|Port Campbell Limestone|60299|5|Briefly described|p228 Tb.5|Miocene|Miocene|Age: 12 Ma. Palaeopole position given.||||||
15462|Port Campbell Limestone|60538|5|Briefly described|p471 Fig. 10|||||||||
15462|Port Campbell Limestone|60563|5|Briefly described|p46|||Of the Heytesbury Group. Overlies the Gellibrand Marl. Shelfal bioclastic calcarenite facies.||||||
15462|Port Campbell Limestone|60785|5|Briefly described|p184 Fig.1, p186, p188.  |Messinian|Langhian|Of the Otway Basin. Foraminifera zones N10-N17(Holdgate and Gallagher, 2003). Has yielded  partial skeletons, and a fairly well-preserved posterior part of the mandible of a fossil cetacean, with two large conical teeth in place.|||Includes Bochara Limestone Member and Muddy Creek Marl Member.|Unconformably underlies the Rocklands Rhyolite.|Yellow fine-grained calcarenite.|
15462|Port Campbell Limestone|61136|6|Mentioned|p18, p27|Miocene|Miocene|Carbonate sediments. Lady Julia Island, which is a volcanic remnant, rests on this unit.||||||
15462|Port Campbell Limestone|61155|5|Briefly described|p18|Late Miocene|Middle Miocene|Of the Heytesbury Group. Contains the Rutledge Marl Member. Overlies Gellibrand Marl. Age: ~15-5.5Ma. Max. thickness: 550m. Geological Province: Otway Basin (Tyrendarra and Port Campbell Embayments).||||||07-MAR-07
15462|Port Campbell Limestone|61181|5|Briefly described|p134|Miocene|Miocene|Comprises limestone, clayey limestone, marl and calcareous clay. Overlies Gellibrand Marl.||||||
15462|Port Campbell Limestone|61182|3|Fully described|p28, p29, p33, p178|Late Miocene|Middle Miocene|Of Heytesbury Group. Formerly subdivided into Rutledges Creek, Port Campbell and Peterborough beds (Baker 1950) also referred to as members. Overlies Gellibrand Marl; usually overlain disconformably by Hanson Plain Sand. Calcisiltite and calcarenite.||||||23-MAY-13
15462|Port Campbell Limestone|61623|6|Mentioned|p449 Fig. 4|Miocene|Miocene|Of Heytesbury Group. Geological Province: Otway Basin.||||||07-APR-09
15462|Port Campbell Limestone|61624|5|Briefly described|p465, p466, p466 Fig. 2|Middle Miocene|Early Miocene|Of Haytesbury Group. Underlain by Clifton Formation. Geological Province: Otway Basin.||||||07-APR-09
15462|Port Campbell Limestone|61626|5|Briefly described|p487, p486 Fig. 2, p489 Fig. 5|Miocene|Miocene|Geological Province: Otway Basin.||||||07-APR-09
15462|Port Campbell Limestone|61628|5|Briefly described|p509 Fig. 3|Late Miocene|Middle Miocene|Of Heytesbury Group. Geological Province: Otway Basin.||||||07-APR-09
15462|Port Campbell Limestone|61896|5|Briefly described|p57|Miocene|Miocene|Locally unconformably overlain by Moorabool Viaduct Formation.||||||19-DEC-07
15462|Port Campbell Limestone|62068|5|Briefly described|p134,135, p135 Fig.2,p136,p137,|Miocene|Miocene|Has karst topography on upper surface.||||Overlain by Whalers Bluff Formation. Unconformably overlain by Hanson Plain Sands. Same as, or equivalent to, Portland Limestone.|Pale yellow, horizontally bedded, shallow marine limestones in Childers Cove.|
15462|Port Campbell Limestone|63269|5|Briefly described|p605|Miocene|Miocene|Otway Basin.||Heytesbury Group.||||
15462|Port Campbell Limestone|66002|4|Described|p13 Tb.9, p26 Fig.7|Neogene|Neogene|Of Heytesbury Group. Modified from Port Campbell Beds of Baker (1950). Defined by Glenie 1971. Calcarenite, minor calcilutite, generally fine-grained. Minor coarse-grained calcarenite, quartz sand and clayey silt. Weakly cemented. Moderately well bedded. Some fossils||||||
15462|Port Campbell Limestone|66012|4|Described|p18|Miocene|Miocene|Of Heytesbury Group. Overlies Gellibrand Marl. Early to middle Miocene|| ||||13-JUN-13
15462|Port Campbell Limestone|66245|5|Briefly described|p6 Fig.5. |Messinian|Serravallian|||Unit in Heytesbury Group.||Overlies Gellibrand Marl.||
15462|Port Campbell Limestone|67061|6|Mentioned|p546 Fig.3.|Miocene|Miocene|||Unit in Heytesbury Group.||||
15462|Port Campbell Limestone|67366|5|Briefly described|p103 Fig.2. |Miocene|Miocene|||Unit in Heytesbury Group.||Overlies Gellibrand Marl.|Shallow to open marine limestone.|
15462|Port Campbell Limestone|67367|5|Briefly described|p131 Fig.2. |Late Miocene|Middle Miocene|||Unit in Heytesbury Group.||||
15462|Port Campbell Limestone|68116|5|Briefly described|Appendix, Maps 47-49, 54-55.|Miocene|Miocene||||||Calcarenite, minor calcilutite: generally fine-grained; bryozoan, mollusc, echinoid and brachiopod fragments, minor coarse-grained calcarenite, quartz sand and clayey silt; weakly cemented, moderately bedded; continental shelf deposit.|
15462|Port Campbell Limestone|68991|5|Briefly described|p465, p465 Fig.2, p466|Miocene|Miocene|Cliff-forming unit with a middle to upper Miocene age. Maximum thickness: 297 m. An irregular solution surface occurs on the Port Campbell Limestone.||||Conformably underlain by the Gellibrand Marl. Disconformably overlain by the Hesse Clay. Unconformably overlain by the Hanson Plain Sand. Disconformably overlain by the Bridgewater Formation.|Comprises marine, grey to yellow calcisiltite to fine-grained calcarenite with minor interbeds of medium- to coarse-grained calcarenite.|
15462|Port Campbell Limestone|69297|5|Briefly described|p79, p98|Serravallian|Serravallian|Otway Basin.||Heytesbury Group||Overlies the Gellibrand Marl. Unconformably overlain by the Hanson Plain Sand.|Limestones.|
15462|Port Campbell Limestone|69651|5|Briefly described|p10|Miocene|Miocene|||Heytesbury Group.||Overlies Gellibrand Marl. Is overlain unconformably by Hanson Plain Sand.||
15462|Port Campbell Limestone|70077|5|Briefly described|Nelson: Fig.2. Regional: Fig.4|Miocene|Miocene|Otway Basin: Port Campbell Embayment.||Heytesbury Group.||Overlies Gellibrand Marl. Is overlain by Hanson Plain Sand.||
15462|Port Campbell Limestone|70880|6|Mentioned|p77|Miocene|Miocene|Otway Basin.||||||
15462|Port Campbell Limestone|70909|6|Mentioned|p63|||||||||
15462|Port Campbell Limestone|70942|4|Described|p127, 119|||See correlation table.||||||
15462|Port Campbell Limestone|71266|6|Mentioned|p614 Fig.3|Miocene|Miocene|Otway Basin.||||||
15462|Port Campbell Limestone|71419|6|Mentioned|p16 Fig 17|Miocene|Miocene|Shallow marine sediments.||||||
15462|Port Campbell Limestone|71437|4|Described|Fig. 1 opp 154, p155, p161-162|Miocene|Miocene|marine, deep neritic.||Of Heytesbury Group.||Laterally continuous with Portland Limestone Member.|Pure to marly limestone, minor chert.|
15462|Port Campbell Limestone|72445|5|Briefly described|App.1, App.2.|||App.2 is a .csv format file. Identified in Stavely 01.||Heytesbury Group||Conformably overlies Gellibrand Marl. Conformably overlain by Loxton Sand.|Includes sandy to muddy calcareous marl with some muddier sections and abundant shell fragments in Stavely 01.|
15462|Port Campbell Limestone|73357|5|Briefly described|p30, p46, p48|Tortonian|Langhian|Otway Basin. Correlated with Operculodinium Dinocyst Superzone and Triporopollenites bellus Spore-Pollen Zone, nearshore to offshore marine depositional environments.||Of Heytesbury Group.||Overlies Gellibrand Marl.||
15462|Port Campbell Limestone|73383|5|Briefly described|p2-3, p10 Tb.3.8, p25, p28, p164, p236|Miocene|Miocene|Otway Basin. Approximately equivalent to chemostratigraphic package S6-P4 which has high Ca, Cr/Nb and Sc/Rb values. Includes limestone and Fe-shale based on geochemistry. See also vi, p11 Tb.3.9, p34, p107, p130, p257.||Heytesbury Group||Overlies Gellibrand Marl|Limestones.|
15462|Port Campbell Limestone|73385|5|Briefly described|p5|Miocene|Miocene|Otway Basin.||Heytesbury Group||Overlies Gellibrand Marl, underlies Bridgewater Formation.|Shallow to open marine limestones.|
15462|Port Campbell Limestone|73386|5|Briefly described|p4, p6, p14, Attachment A1|Tortonian|Langhian|Otway Basin. Shallow to open marine depositional environments, outer shelf water depths during peak transgressions and at mid to inner shelf depths during regressions. Upper part records continuous sea level fall. Correlates with Triporopollenites bellus Spore-Pollen Zone.||Heytesbury Group||Overlies Gellibrand Marl|Limestones.|
15462|Port Campbell Limestone|73486|4|Described|p509-514, p516-523, p525-531, p533-535|Messinian|Serravallian|Otway Basin. Thickness of up to 297 m in the Port Campbell Embayment. Gradational transition with Gellibrand Marl. Contains decametre-scale cycles, and thin repetitive third-order cycles of shoaling-upward character. Oxic-suboxic to euxinic/anoxic depositional environment. Common to abundant foraminifera of middle to outer shelf species, and inner to middle shelf species in upper part. Sequence was emergent at ca 13.2 Ma. Uppermost weathered surface is a pisolitic ferricrete crust atop oxidised ferruginous carbonate sand.|15-10.5 Ma (foraminifera)|Heytesbury Group||Overlies Gellibrand Marl with gradational transition, underlies Hesse Clay|Grey fine-grained unconsolidated to semi-consolidated bioclastic muddy carbonate sands and limey marls, uniform appearance, upper weathered zone. Predominantly calcite, minor siliciclastics and glauconitic carbonate mud. Texturally variable.|
15462|Port Campbell Limestone|73594|5|Briefly described|p4|Miocene|Miocene|Otway Basin.||Heytesbury Group||Overlies Gellibrand Marl|Marine limestones.|
15472|Port Julia Greensand|23671|6|Mentioned|p2|||||||||
15472|Port Julia Greensand|23768|5|Briefly described|p28 Fig.5|Oligocene|Oligocene|Presented as Port Julia only in figure.||||||29-MAR-05
15472|Port Julia Greensand|23818|5|Briefly described|p174 Fig.84|Late Eocene|Late Eocene|Port is spelt Pt. in text.||||||
15472|Port Julia Greensand|29833|6|Mentioned|p142|||||||||
15472|Port Julia Greensand|30251|4|Described|p4|||Also mention P3, refs Steel(1961)||||||
15472|Port Julia Greensand|33330|6|Mentioned|p164|||Refers Ludbrook (1963).||||||
15472|Port Julia Greensand|34308|6|Mentioned|Fig.84|||Aldingan. Correlation chart||||||
15472|Port Julia Greensand|38068|6|Mentioned|Fig.7|||||||||
15472|Port Julia Greensand|40238|6|Mentioned|Fig.2|||||||||
15472|Port Julia Greensand|41513|5|Briefly described|p45|||||||||
15472|Port Julia Greensand|41517|6|Mentioned|p139|||||||||
15472|Port Julia Greensand|41626|6|Mentioned|p54|||||||||
15472|Port Julia Greensand|44691|4|Described|map legend|Miocene|Oligocene|Defn on Tech.File (I/53-12). Oligocene-Miocene.||||||
15472|Port Julia Greensand|67462|5|Briefly described|Map legend.|Oligocene|Oligocene|Western Saint Vincent Basin.||||||
15497|Potosi Gneiss|22959|6|Mentioned|p95||Paleoproterozoic|||||||07-NOV-08
15497|Potosi Gneiss|22961|6|Mentioned|p80||Paleoproterozoic|||||||07-NOV-08
15497|Potosi Gneiss|23461|5|Briefly described|p202|||||||||
15497|Potosi Gneiss|32657|6|Mentioned|p117|||||||||
15497|Potosi Gneiss|33262|5|Briefly described|PB222|||||||||
15497|Potosi Gneiss|35170|6|Mentioned|Fig.2|||||||||
15497|Potosi Gneiss|37461|6|Mentioned|p321|||||||||
15497|Potosi Gneiss|37581|6|Mentioned|p74|||||||||
15497|Potosi Gneiss|39883|6|Mentioned|p381|||||||||
15497|Potosi Gneiss|40448|6|Mentioned|p30|||||||||
15497|Potosi Gneiss|40852|5|Briefly described|p23|||||||||
15497|Potosi Gneiss|41145|6|Mentioned|Fig.5|||||||||
15497|Potosi Gneiss|41633|6|Mentioned|Fig.2.7|||||||||
15497|Potosi Gneiss|41870|6|Mentioned|p120|||||||||
15497|Potosi Gneiss|43610|6|Mentioned|p19|||1690+/-5 Ma (Zircon U-Pb)||||||
15497|Potosi Gneiss|45003|14|Not recorded|p333|||||||||
15497|Potosi Gneiss|45166|5|Briefly described|p25|||||||||
15497|Potosi Gneiss|46597|14|Not recorded|p187|||||||||
15497|Potosi Gneiss|46601|14|Not recorded|p.320,323|||Fig.7.||||||
15497|Potosi Gneiss|64316|5|Briefly described|p533 Fig. 1|||Reference also made to 'Possi-type gneiss'.  Geological Province: Broken Hill Block. This is a garnet-rich variant of the Hores Gneiss.||||||07-FEB-11
15497|Potosi Gneiss|64896|6|Mentioned|p1392 Fig. 3|||Geological Province: Curnamona Province.||||||
15497|Potosi Gneiss|68126|6|Mentioned|p26|||Apparently related to a c.1690 Ma thermal event.||||||
15525|Pound Subgroup|7931|5|Briefly described|p99 Fig. 2|Ediacaran|Ediacaran|Comprises Rawnsley Quartzite and Bonney Sandstone. Overlain by Parachilna Formation.||||||07-FEB-11
15525|Pound Subgroup|22646|6|Mentioned|Fig 4 on p 102|Neoproterozoic|Neoproterozoic|Adelaide Geosyncline (West).  Age - Ediacarian in text.||||||
15525|Pound Subgroup|22772|5|Briefly described|Table 13.1|Neoproterozoic III|Neoproterozoic III|||||||
15525|Pound Subgroup|22857|5|Briefly described|Tb. 13.1 (insert p70-71)|Precambrian|Precambrian|Of the Wilpena Group. Age: >545Ma.||||||24-MAR-06
15525|Pound Subgroup|22901|6|Mentioned|76 fig 2|||Geol province Adelaide Rift Complex||||||
15525|Pound Subgroup|22927|6|Mentioned|43|||Geol province Adelaide Geosyncline||||||
15525|Pound Subgroup|22949|5|Briefly described|p27|Neoproterozoic|Neoproterozoic|Of Wilpena Group. Contains Ediacara assemblage of soft-bodied metazoan fossils.||||||13-FEB-08
15525|Pound Subgroup|23211|6|Mentioned|Fig.1,2|||Of Wilpena Group.||||||20-JAN-09
15525|Pound Subgroup|23282|6|Mentioned|p65|||May correlate with Narana Formation. of Adelaide Fold Belt.||||||
15525|Pound Subgroup|23287|6|Mentioned|Fig.3|||Age: Upper Ediacarian. of Wilpena Group.||||||
15525|Pound Subgroup|23445|5|Briefly described|p436 Fig.1|||Of Wilpena Group.||||||19-NOV-07
15525|Pound Subgroup|23557|5|Briefly described|p95 Fig.1|Neoproterozoic III|Neoproterozoic III|Geological Province: Adelaide Rift Complex.||||||
15525|Pound Subgroup|23806|6|Mentioned|p1122|||||||||
15525|Pound Subgroup|24586|5|Briefly described|p51 Fig. 1, p52 Fig. 3|Adelaidean|Adelaidean|Of the Wilpena Group (Heysen Supergroup). Includes Bonney Sandstone and Rawnsley Quartzite. Geological Province: Adelaide Geosyncline.||||||05-JUL-06
15525|Pound Subgroup|36011|6|Mentioned|p13|||||||||
15525|Pound Subgroup|36731|6|Mentioned|p121|||||||||
15525|Pound Subgroup|37015|6|Mentioned|Fig.2|||||||||
15525|Pound Subgroup|37461|6|Mentioned|Table 5.I|||||||||
15525|Pound Subgroup|37627|6|Mentioned|p185|||||||||
15525|Pound Subgroup|38004|6|Mentioned|p81|||See also P82.||||||
15525|Pound Subgroup|38157|6|Mentioned|Table 1|||See also Table V.||||||
15525|Pound Subgroup|38330|6|Mentioned|p217|||||||||
15525|Pound Subgroup|38970|6|Mentioned|p105|||||||||
15525|Pound Subgroup|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Marinoan||||||
15525|Pound Subgroup|39490|6|Mentioned|Fig.1(6)|||||||||
15525|Pound Subgroup|39808|6|Mentioned|p223|||||||||
15525|Pound Subgroup|40537|6|Mentioned|p328|||||||||
15525|Pound Subgroup|40852|6|Mentioned|Fig.3.2|||||||||
15525|Pound Subgroup|40906|6|Mentioned|Fig.9|||||||||
15525|Pound Subgroup|41001|6|Mentioned|p169|||||||||
15525|Pound Subgroup|41236|6|Mentioned|Fig.2|||||||||
15525|Pound Subgroup|41400|6|Mentioned|p27|||||||||
15525|Pound Subgroup|41401|6|Mentioned|p33|||||||||
15525|Pound Subgroup|41424|5|Briefly described|p299|||||||||
15525|Pound Subgroup|41429|4|Described|p242|||||||||
15525|Pound Subgroup|41457|6|Mentioned|Fig.1|||||||||
15525|Pound Subgroup|41496|6|Mentioned|p52|||||||||
15525|Pound Subgroup|41500|6|Mentioned|Fig.1|||||||||
15525|Pound Subgroup|41526|6|Mentioned|p3|||||||||
15525|Pound Subgroup|41801|6|Mentioned|p219|||||||||
15525|Pound Subgroup|42011|6|Mentioned|p457|||||||||
15525|Pound Subgroup|42028|6|Mentioned|p137|||||||||
15525|Pound Subgroup|42098|6|Mentioned|Table 2 P54|||||||||
15525|Pound Subgroup|42192|6|Mentioned|Fig.8 P17|||||||||
15525|Pound Subgroup|42222|6|Mentioned|p18|||||||||
15525|Pound Subgroup|42240|6|Mentioned|Fig.2 P165|||||||||
15525|Pound Subgroup|42241|6|Mentioned|p179|||||||||
15525|Pound Subgroup|42272|6|Mentioned|Fig.2 P400|||||||||
15525|Pound Subgroup|42444|5|Briefly described|Fig.2 P16|||||||||
15525|Pound Subgroup|42643|6|Mentioned|p21|||Adelaide Geosyncline||||||
15525|Pound Subgroup|42813|6|Mentioned|p22|||of Wilpena Group||||||
15525|Pound Subgroup|42882|5|Briefly described|Table 1 P3|||Of Wilpena Group.||||||19-NOV-07
15525|Pound Subgroup|43052|4|Described|p194,table 6.1|||Of Wilpena  Group.||||||19-NOV-07
15525|Pound Subgroup|43845|5|Briefly described|Fig2 p42||Neoproterozoic|In Wilpena Group.||||||12-JUL-16
15525|Pound Subgroup|44133|5|Briefly described|p22, 31|||||||||
15525|Pound Subgroup|60718|6|Mentioned|p50 Tb. 1|||Geological Province: Adelaide Geosyncline. Of Hawker Group, Frome diapir.||||||09-NOV-10
15525|Pound Subgroup|60889|6|Mentioned|p250 Fig.7|||||||||
15525|Pound Subgroup|60953|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Shallow marine sandstone.||||||
15525|Pound Subgroup|60959|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Of the Wilpena Group.||||||
15525|Pound Subgroup|61108|5|Briefly described|map legend|Adelaidean|Adelaidean|Shallow marine sandstone; contains metazoan fossils.||||||06-JUN-05
15525|Pound Subgroup|61732|5|Briefly described|p4 Fig. 3|Marinoan|Marinoan|Of the Wilpena Group. Includes the ~556+/-24Ma Bonney Sandstone. Geological Province: Adelaide Rift Complex/Stuart Shelf. See also p156 Fig. 58.||||||07-FEB-11
15525|Pound Subgroup|62085|6|Mentioned|p19 Fig.4|Ediacaran|Ediacaran|Hosts the Ediacara fauna.||Wilpena Group|Includes Rawnsley Quartzite.||Sandstone, quartzite, siltstone.|
15525|Pound Subgroup|62453|5|Briefly described|p12 Fig. 8|Ediacaran|Ediacaran|Geological Province: Adeliade Rift Complex/Stuart Shelf.||||||
15525|Pound Subgroup|62664|5|Briefly described|p138 Fig.2.|Neoproterozoic|Neoproterozoic|||Unit in Wilpena Group.|||Sandstone.|
15525|Pound Subgroup|62903|6|Mentioned|p730 Fig.1|Ediacaran|Ediacaran|Adelaide Rift Complex. Presented in figure as Pound.||||overlies Wonoka Formation||
15525|Pound Subgroup|63458|6|Mentioned|p897 Fig.19. |Ediacaran||||Unit in Wilpena Group.|Includes Billy Springs Formation ?|||12-JUN-15
15525|Pound Subgroup|64455|5|Briefly described|p138 Fig. 1, p140|Early Cambrian|Ediacaran|Of Wilpena Group. Includes Bonney Sandstone and Rawnsley Quartzite. Underlain by Wonoka Formation.||||||29-JAN-09
15525|Pound Subgroup|64460|6|Mentioned|p195|||Includes Rawnsley Quartzite.||||||
15525|Pound Subgroup|64829|5|Briefly described|p1084 Fig. 1|Neoproterozoic|Neoproterozoic|||||||07-FEB-11
15525|Pound Subgroup|65313|6|Mentioned|p576 Fig. 5|Neoproterozoic|Neoproterozoic|||||Overlies Wonoka Formation.||26-MAR-12
15525|Pound Subgroup|65365|5|Briefly described|p10 Fig. 4|Ediacaran|Ediacaran|Adelaide Rift Complex / Stuart Shelf. Includes Bonney Sandstone Member dated at 556 +/- 24 Ma (Preiss, 2000).  Includes Ediacara fauna.||||||19-MAR-12
15525|Pound Subgroup|65366|5|Briefly described|p23 Fig. 3|Ediacaran|Ediacaran|Adelaide Rift Complex / Stuart Shelf. Includes Bonney Sandstone Member dated at 556 +/- 24 Ma (Preiss, 2000). Includes Ediacara fauna.||||||19-MAR-12
15525|Pound Subgroup|65376|6|Mentioned|p140 Fig.4.22.|Neoproterozoic|Neoproterozoic|||||||
15525|Pound Subgroup|65925|5|Briefly described|Appendix 2.||||||||Sandstone; quartzite; siltstone.|
15525|Pound Subgroup|66522|6|Mentioned|p23.|||||||||
15525|Pound Subgroup|67484|5|Briefly described|p294 Tb.1, p299 Tb.2|Ediacaran|Ediacaran|Adelaide Rift Complex.|||Includes Bonney Sandstone and Rawnsley Quartzite.|Is overlain by Hawker Group.||26-MAY-15
15525|Pound Subgroup|67620|5|Briefly described|p5|Ediacaran|Ediacaran|Adelaide Rift Complex.||Wilpena Group.|Bonney Sandstone, Rawnsley Quartzite.|Overlies Wonoka Formation. Is overlain by Hawker Group.||
15525|Pound Subgroup|67870|5|Briefly described|p9|Ediacaran|Ediacaran|Adelaide Rift System.||Wilpena Group.|Bonney, Rawnsley Formations.|||
15525|Pound Subgroup|68030|5|Briefly described|p239|Cambrian|Ediacaran|Flinders Ranges.|||Includes Rawnsley Quartzite, Ediacara Member, Chace Quartzite Member and Bonney Sandstone.|||
15525|Pound Subgroup|68138|6|Mentioned|p156|Neoproterozoic|Neoproterozoic|Adelaide Rift Complex.|||Bonney Sandstone, Rawnsley Quartzite.|||
15525|Pound Subgroup|68271|5|Briefly described|p693|||Comprises the upper part of the stratotypic Ediacaran System in the western central Flinders Ranges (Preiss 2005; Knoll et al. 2006).||||||
15525|Pound Subgroup|68473|6|Mentioned|p531|||Adelaide Rift Complex.||||||
15525|Pound Subgroup|69019|5|Briefly described|p54, p61-63.|Late Neoproterozoic|Late Neoproterozoic|After Pound Quartzite (Mawson, 1938); further defined by Forbes (1971), whose Bonney Sandstone Member and Rawnsley Quartzite Member were elevated to Formation status (in the Pound Subgroup) by Jenkins (1975). Central and northern Flinders Ranges. Thickness >3,000 m. Hosts the Ediacaran Faunal Assemblage and GSSP.||Unit in Wilpena Group.||Conformably overlies Wonoka Formation.||
15525|Pound Subgroup|70031|5|Briefly described|p243,245|Ediacaran|Ediacaran|Adelaide Geosyncline. Hosts Ediacara biota (oldest, definitive large, soft-bodied organisms) in shallow-marine arenites.||Unit of Wilpena Group.|Includes Rawnsley Quartzite and Bonney Sandstone.|Upper unit of Wilpena Group. Underlain by Wonoka Formation.||
15525|Pound Subgroup|70334|5|Briefly described|p30,56,78|Neoproterozoic|Neoproterozoic|Geological province: Gawler Craton. Of Adelaide Geosyncline and Stuart Shelf. Completely eroded from the Flinders Ranges during Cambrian uplift. Exposed at Devil's Peak on the Augusta sheet.|||Includes Rawnsley Quartzite.|||14-OCT-19
15525|Pound Subgroup|70384|5|Briefly described|Map legend.|Ediacaran|Neoproterozoic|Adelaide Geosyncline.|||Bonney Sandstone, Rawnsley Quartzite, Billy Springs Formation.|||
15525|Pound Subgroup|70406|6|Mentioned|p127|||||||||
15525|Pound Subgroup|70407|5|Briefly described|p102 Fig 1, p103 Fig 2, p111, 112|Neoproterozoic|Neoproterozoic|Age: Ediacaran. More work required to subdivide the Group into Subgroups.||Of Wilpena Group.|Includes Bonney Sandstone, Rawnsley Quartzite, Wilyerpa Formation,Tindelpina Shale,  Tapley Hill Formation,|||
15525|Pound Subgroup|70790|5|Briefly described|p258 Fig.1|Ediacaran|Ediacaran|Adelaide Rift Complex.||Wilpena Group.|Bonney Sandstone, Rawnsley Quartzite.|||
15525|Pound Subgroup|71129|6|Mentioned|p128|Ediacaran|Ediacaran|Of Adelaide Geosyncline.||Unit of Wilpena Group.||||
15525|Pound Subgroup|71250|6|Mentioned|p69-70|Ediacaran|Ediacaran|Central Flinders Ranges.||Wilpena Group.|Bonney Sandstone, Rawnsley Quartzite.|||
15525|Pound Subgroup|73093|5|Briefly described|map legend|Neoproterozoic|Neoproterozoic||||||Sandstone; quartzite; siltstone.|09-DEC-21
15525|Pound Subgroup|73110|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic||||||Sandstone; quartzite; siltstone.|
15525|Pound Subgroup|73188|6|Mentioned|p315, p352|||Flinders Ranges.||||||
15525|Pound Subgroup|73222|6|Mentioned|p6, p11-12, p16-17, p24|Ediacaran|Ediacaran|Adelaide Rift Complex.||Wilpena Group, Heysen Supergroup|Rawnsley Quartzite, Bonney Sandstone, Patsy Hill Member|||
15525|Pound Subgroup|74367|5|Briefly described|p7 Fig.6, p8, p22|Ediacaran|Ediacaran|||Wilpena Group|Bonney Sandstone, Rawnsley Quartzite, Billy Springs Quartzite|||
15555|Pretty Hill Formation|12781|6|Mentioned|p386|Early Cretaceous|Early Cretaceous|Otway Basin. Maximum thickness 1585m.||Crayfish Group.||Unconformably overlies Casterton Formation. Is overlain by Laira Formation.||
15555|Pretty Hill Formation|22480|6|Mentioned|5||Early Cretaceous|Otway Basin||||||
15555|Pretty Hill Formation|22495|6|Mentioned|P220|||||||||
15555|Pretty Hill Formation|22674|4|Described|p718, Fig.2 p719|Barremian|Berriasian|||||||
15555|Pretty Hill Formation|22686|6|Mentioned|Fig3p745,747|Hauterivian|Portlandian|Max Age: 141 Ma; Min Age: 123 Ma.  Geological Province: Otway Basin.||||||17-JAN-06
15555|Pretty Hill Formation|22875|3|Fully described|p33|Aptian|Valanginian|Of the Crayfish Group||||||18-FEB-08
15555|Pretty Hill Formation|22924|5|Briefly described|51|||||||||
15555|Pretty Hill Formation|22930|6|Mentioned|50|||||||||
15555|Pretty Hill Formation|23356|5|Briefly described|26 Tab.2|Early Cretaceous|Late Jurassic|||||||
15555|Pretty Hill Formation|23427|5|Briefly described|Table 11.2 p418.|||||||||
15555|Pretty Hill Formation|24209|5|Briefly described|p151|Valanginian|Berriasian|Comprises interbedded litharenties and shales.  See also p158 Fig. 7.||||||
15555|Pretty Hill Formation|24314|5|Briefly described|p61 Fig.2|Early Cretaceous|Early Cretaceous|Geological Province: Otway Basin. Max. Thickness ?5000m. Of the Otway Supergroup.||||||30-NOV-04
15555|Pretty Hill Formation|24453|5|Briefly described|p809 Fig.2|Hauterivian|Berriasian|Of Crayfish Subgroup. Geological Province: Otway Basin.||||||07-FEB-11
15555|Pretty Hill Formation|24562|5|Briefly described|p8 Fig. 2|Early Cretaceous|Early Cretaceous|Of the Crayfish Group.  Geological Province: Otway Basin.||||||
15555|Pretty Hill Formation|41269|5|Briefly described|p244|||||||||
15555|Pretty Hill Formation|41454|6|Mentioned|Fig.6|||||||||
15555|Pretty Hill Formation|41714|6|Mentioned|Fig.2|||||||||
15555|Pretty Hill Formation|42075|5|Briefly described|Fig.13 P252|||||||||
15555|Pretty Hill Formation|42150|6|Mentioned|p69|||||||||
15555|Pretty Hill Formation|42153|5|Briefly described|p352|||See also Fig.2||||||
15555|Pretty Hill Formation|43171|6|Mentioned|5-8|||Of Crayfish Group. Age: 135-145 Ma||||||
15555|Pretty Hill Formation|43195|5|Briefly described|Map Legend||Early Cretaceous|See also commentary on back of map.Of Crayfish Group.||||||
15555|Pretty Hill Formation|43219|5|Briefly described|Fig.3,p6.|Aptian|Valanginian|Of Otway Group.||||||16-DEC-08
15555|Pretty Hill Formation|43744|6|Mentioned|Fig.3,p3|||||||||
15555|Pretty Hill Formation|43937|5|Briefly described|Map Legend|Aptian|Kimmeridgian|||||||
15555|Pretty Hill Formation|44133|5|Briefly described|p144|Early Cretaceous|Early Cretaceous|Previously called 'Geltwood Beach Formation'. Thickness: 1585m.||||||
15555|Pretty Hill Formation|50154|6|Mentioned|p44|||Also known as the Crayfish Subgroup.||||||
15555|Pretty Hill Formation|60126|6|Mentioned|p4|||Basal unit overlain by Casterton Formation?||||||25-JAN-06
15555|Pretty Hill Formation|60452|6|Mentioned|p14|Late Cretaceous|Late Jurassic|Outwash fan and braided stream deposits. In the Bassian Rift.||||||
15555|Pretty Hill Formation|60599|6|Mentioned|p84|||Outwash fan and braided stream deposits. Geological Province: Otway Basin.||||||
15555|Pretty Hill Formation|61017|5|Briefly described|p5 Fig. 2|Barremian|Bernasian|Of the Crayfish Subgroup (Otway Group). Includes shales with hydrocarbon potential as source rocks. Geological Province: Otway Basin.||||||07-FEB-11
15555|Pretty Hill Formation|61182|3|Fully described|p11-12, p72|Aptian|Valanginian|Of Otway Group.Together with Eumeralla Formation, unconformable over Casterton Formation or over palaeozoic bedrock; unconformably overlain by Eumeralla Formation. Mainly quartz sandstone (lower part) with minor mudstone (upper). Geol.Prov: Otway Basin.||||||04-FEB-08
15555|Pretty Hill Formation|61185|5|Briefly described|p56|Early Cretaceous|Late Jurassic|Deposits of scree, outwash fan and braided streams (Tickell et al. 1992). Geological Province: Otway Basin.||||||07-FEB-11
15555|Pretty Hill Formation|61470|5|Briefly described|p28 Fig. 5|Barremian|Berriasian|Of the Crayfish Subgroup (Otway Group). Underlies Laira Formation. Geological Province: Otway Basin.||||||12-OCT-05
15555|Pretty Hill Formation|61547|6|Mentioned|p461 Fig.2, p462, p465, p468, p472.|Valanginian|Berriasian|||Basal unit in Crayfish Group.|Includes Lower and Upper Sawpit Shale Members, Sawpit Sandstone Member, and Pretty Hill Sandstone Member.|Overlies Casterton Formation. Is overlain by Laira Formation.||
15555|Pretty Hill Formation|61618|6|Mentioned|p425, p433|||Laterally variable braided-fluvial deposit.||||||
15555|Pretty Hill Formation|61622|5|Briefly described|p436 Fig. 2|Cretaceous|Cretaceous|Of Crayfish Group. Geological Province: Otway Basin.||||||07-FEB-11
15555|Pretty Hill Formation|61623|6|Mentioned|p447, p451, p449 Fig. 4|Early Cretaceous|Early Cretaceous|Of Crayfish Group. Geological Province: Otway Basin.||||||07-APR-09
15555|Pretty Hill Formation|61626|5|Briefly described|p486 Fig. 2|Early Cretaceous|Early Cretaceous|Of Crayfish Group. Geological Province: Otway Basin.||||||07-APR-09
15555|Pretty Hill Formation|61627|5|Briefly described|p500 Fig. 2|Early Cretaceous|Early Cretaceous|Of Crayfish Group. Overlian by Laria Formation, Underlain by Casterton Formation. Geological Province: Otway Basin.||||||07-FEB-11
15555|Pretty Hill Formation|61628|5|Briefly described|p509 Fig. 3|Early Cretaceous|Early Cretaceous|Of Crayfish Subgroup. Geological Province: Otway Basin.||||||07-APR-09
15555|Pretty Hill Formation|63122|5|Briefly described|p17 Fig. 4.3|Hauterivian|Berriasian|Of the Crayfish Group. Max. thickness: >1585m. Geological Province: Otway Basin.||||||
15555|Pretty Hill Formation|63124|3|Fully described|p48 Fig. 5.1, p49 Fig. 5.2, p58-59|Valanganian|Berriasian|Of Crayfish Gp (Otway Supergp). Unconformable on Casterton Fm; conformable below Laira Fm. Contains mineralogically complex grey-green litharenite to feldspathic litharenite with siltstone interbeds. Age:140-133Ma. Max.thick:?5000m. Geol.Prov: Otway Basin||||||
15555|Pretty Hill Formation|63125|5|Briefly described|p105, p116 Tb. 7.6|||Overlies the Casterton Formation. Geological Province: Otway Basin. Basal section predominantly more shaly and referred to as "unnamed basal shale"; remainder of formation comprises interbedded sandstone, siltstone and shale with rare coal laminae.||||||
15555|Pretty Hill Formation|63129|5|Briefly described|p127|Early Cretaceous|Early Cretaceous|Of the Otway Supergroup. Thickness: up to 875m in Ladbroke Grove 1. Geological Province: Otway Basin. Good porosity which creates good reservoir conditions.||||||17-JUN-09
15555|Pretty Hill Formation|63130|5|Briefly described|p141|||Of the Crayfish Group. Geological Province: Otway Basin.||||||06-FEB-08
15555|Pretty Hill Formation|63267|5|Briefly described|p483-486, p491-493, p495-497|Early Cretaceous|Early Cretaceous|Main reservoir in the Penola Trough, Otway Basin; also source potential (elaborated). Low-sinuosity braided-fluvial deposits. Wireline log. Apparently regarded as interchangeable with Pretty Hill Sandstone (see references p488-490, p492-495). Also appears as Pretty Formation on p495. Significance of faults discussed.||Crayfish Group.||Unconformably overlies Casterton Formation. Is overlain transitionally by Laira Formation.|Grey-green litharenites to feldspathic litharenites.|
15555|Pretty Hill Formation|63269|5|Briefly described|p604-605, p607, p616, p618|Early Cretaceous|Early Cretaceous|Otway Basin. Most of this unit in the Penola Trough axis has remained in the gas generation window since latest Cretaceous. Details of natural gas, oils and oil stains in named wells tabulated. Oil-source correlation. Biomarker diagram. Appears as Pretty Hill Sandstone on p606.||Crayfish Subgroup.||||
15555|Pretty Hill Formation|63431|5|Briefly described|p676, p677 Fig. 2|Valanginian|Berriasian|Basal unit of the Crayfish Group. Geological Province: Penola Trough/Otway Basin. See also p680.||||||07-FEB-11
15555|Pretty Hill Formation|66245|5|Briefly described|p6 Fig.5. |Barremian|Berriasian|Also witten as Pretty Hill sst.||Unit in Crayfish Subgroup.||Is overlain by Laira Formation.|Includes porous sandstones.|
15555|Pretty Hill Formation|67367|5|Briefly described|p131 Fig.2, p132. |Barremian|Berriasian|Has fair hydrocarbon source rock potential, with an average total organic carbon content of 1.7%.||Unit in Crayfish Subgroup.||Is overlain conformably by Laira Formation.||
15555|Pretty Hill Formation|67541|6|Mentioned|p76, p76 Fig.1, p79, p85|||Of the Katnook reservoir (Otway Basin Australia).|||||Comprises chlorite/zeolite-rich sandstone.|
15555|Pretty Hill Formation|69297|5|Briefly described|p79, p98, p100, p101, p104|Hauterivian|Hauterivian|Otway Basin.||Crayfish Subgroup||Overlies the Sawpit Shale and Sawpit Sandstone. Overlain by the Laira Formation.|Siltstone.|
15555|Pretty Hill Formation|69651|5|Briefly described|p10|Early Cretaceous|Early Cretaceous|||Crayfish Subgroup.||Unconformably overlies Casterton Formation. Is overlain by Laira Formation.||
15555|Pretty Hill Formation|69948|6|Mentioned|Fig.4.2|||Otway Basin (a rift basin). Sediment thickness, sonic log, gamma ray log all shown in contrast with Eromanga Basin (an intracratonic basin).||||Is overlain by Laira Formation.||
15555|Pretty Hill Formation|70077|5|Briefly described|Nelson: Fig.2. Regional: Fig.4; p4, p8-9|Early Cretaceous|Early Cretaceous|See also Regional: p11-12. Otway Basin: Port Campbell Embayment and Robe-Penola Trough. Predominantly fluvial sediments. A major play fairway in SA part of Otway Basin; a producing unit in Katnook, Ladbroke Grove, Haselgrove and Haselgrove South gas fields. Good reservoir characteristics in Victoria. Sealed by Eumeralla Formation.||Crayfish Subgroup.||Overlies Casterton Formation or Sawpit Shale/Sawpit Sandstone. Is overlain by Eumeralla or Laira Formation.||
15555|Pretty Hill Formation|70379|5|Briefly described|p717, p719, p722-729, p731-732|Early Cretaceous|Early Cretaceous|Otway Basin. Widespread distribution across the Basin. Appears as Pretty Hill Sst in Fig.2. Isopach map. Relationship of tectonic activity to sediment accumulation discussed in detail. Late Valanginian to Hauterivian. Shown as Pretty Hill Sandstone in Fig2 p719.|c. 136-133 Ma.|Crayfish Group.||Overlies McEachern Sandstone and Sawpit Sandstone (equivalent). Is overlain by Laira Formation, but replaces it (as a lateral equivalent) in the E of the Basin.|Fluvial sediments.|16-FEB-17
15555|Pretty Hill Formation|70880|6|Mentioned|p77|Hauterivian|Berriasian|Otway Basin.||||||
15555|Pretty Hill Formation|71266|6|Mentioned|p614 Fig.3|Early Cretaceous|Early Cretaceous|Otway Basin.||||||
15555|Pretty Hill Formation|71342|6|Mentioned|Ch4 p9|||Otway Basin.||||||
15555|Pretty Hill Formation|72050|5|Briefly described|p233 Fig.2, 234-235, 239|Hauterivian|Berriasian|Has produced gas flows.||Crayfish Group.|||Basal cross-bedded conglomerate, quartzose sandstones, and floodplain to lacustrine shales.|
15555|Pretty Hill Formation|73356|2|Defined|p. v-1, p4-7, p9-11, p13-17, p20-29|Hauterivian|Valanginian|Otway Basin. Revised unit; restricted to the sedimentary sequence between the Sawpit Formation and the Laira Formation. Basal boundary marked by an increase in volcanogenic lithics and feldspar. The top of the formation is notably more lithic-rich and the unit is overall less mineralogically mature than the Sawpit Formation. Upper boundary with Laira Formation is gradational and may be diachronous. Represents a fluvial-overbank system. Age constraint is from palynologic biostratigraphy; extends from the Upper R. australiensis to Upper F. wonthaggiensis Spore-Pollen Subzones of Partridge (2006). Previously informally named unit 'R' (Edworthy, 1964), then Pretty Hill Sandstone (Reynolds et al., 1966; etc). Assigned its current name by Yu (1988)[?]. No type section was designated; now defined by the reference section in Casterton-1 between 1309.2 m and 1711.2 m. Particularly thick in the Penola Trough where it reaches a maximum thickness of 1079.6 m (Salamander-1). Intersected in 54 wells across the basin; 28 in Victoria. Significantly sandier in some places. Corresponds to the S1-P5 and S1-P6 chemostratigraphic packages of Forbes et al. (2020). [See article for description of geophysical character].||Crayfish Subgroup, Otway Group||Underlain by Sawpit Formation (conformably) and Casterton Formation (unconformably). Overlain by Laira Formation.|Fine- to coarse-grained quartz sandstone with silty, micaceous and carbonaceous shale and mudstone interbeds and a fine- to medium-grained basal sandstone. Includes chlorite, garnet, mica, poor coal, kaolinite, abundant feldspar, and plant traces.|
15555|Pretty Hill Formation|73357|5|Briefly described|p15-17, p43, p45, p47|Barremian|Berriasian|Otway Basin. Sparse, poorly preserved palynomorph assemblages, or barren of palynomorphs. Correlated to the Foraminisporis wonthaggiensis Zone, brackish/marginal marine indicators. Lower part assigned to the Ruffordiaspora australiensis Spore-Pollen Zone, limited new data to confirm this.||Of Crayfish Subgroup.||Overlies Casterton Formation, underlies Lower Eumeralla Formation.|Contains sandy lithologies.|
15555|Pretty Hill Formation|73383|4|Described|p3, p7 Tb.3.1, p11, p15-16, p38, p42-45|Barremian|Berriasian|Otway Basin. Equivalent to chemostratigraphic packages S1-P1 to S1-P6. The tops of packages S1-P4 and S1-P5 are associated with large and abrupt chemical changes, may represent intra-formation unconformities of unknown type. Subdivided into several informal lithology-based subunits (Sawpit Sandstone, Upper and Lower Sawpit Shale, Pretty Hill Sandstone and others). Lithologies based on geochemistry using the ChemLith classification includes mudstone, siltstone, limestone, calcareous limestone, argillaceous and calcareous sandstones; and using the Herron classification (1988) includes shale, wacke, Fe-shale, Fe-sand, lith-arenite, sublith-arenite, quartz arenite, subarkose and arkose. See also vi, p49-55, p64-65, p95, p100-103, p110-112, p167, p171-175, p179-187, p195-198, p224-225, p229-233, p239-241, p282-295, p331-342.||Crayfish Subgroup|Sawpit Sandstone, Upper Sawpit Shale, Lower Sawpit Shale, Pretty Hill Sandstone|Unconformably overlies Casterton Formation, underlies Windermere Sandstone, Laira Formation|Fluvial channel sandstones. Includes lower sand unit and upper sand/shale unit.|
15555|Pretty Hill Formation|73385|5|Briefly described|p5|Barremian|Valanginian|Otway Basin.||Crayfish Subgroup||Overlies Casterton Formation, underlies Laira Formation, Windermere Sandstone.|Fluvial channel sandstones with lower sand unit and upper sand/shale unit.|
15555|Pretty Hill Formation|73386|4|Described|p4, p6, p8, Attachment A1|Hauterivian|Valanginian|Otway Basin. Extends from upper part of the Upper Ruffordiaspora australiensis Spore-Pollen Subzone to the lower part of the Upper Foraminisporis wonthaggiensis Spore-Pollen Subzone. Corresponds to the S1-P5 to S1-P6 chemostratigraphic packages (Eid et al., 2021a). Revised Pretty Hill Formation defined by a reference section in Casterton-1 from 1309.2 m to 1711.2 m.||Crayfish Subgroup||Conformably overlies Sawpit Formation, underlies Laira Formation|Characterised by a fluvial-overbank system with sandstones which are dominantly litharenites with arkose and subarkose signatures. Some fining upwards sequences and sparsely interbedded shales.|
15555|Pretty Hill Formation|73594|4|Described|p3-4, p14-16, p20, p42, p45-46, p48-51|Barremian|Valanginian|Otway Basin. Fluvial. Originally defined in VIC and is an important hydrocarbon reservoir in the SA part of the Penola Trough. Informal subdivision of lower part introduced by Lovibond et al. (1995) and largely followed in this review. Camac and Boult (2008) further subdivided the Sawpit Shale. See also p8, p53-54, p59, p64, p66.||Crayfish Subgroup|McEachern Sandstone, Sawpit Shale, Sawpit Sandstone, Pretty Hill Sandstone|Overlies Casterton Formation, underlies Katnook Sandstone, Laira Formation, Windermere Sandstone|Includes fine to medium grained sandstones, moderately sorted litharenites and feldspathic litharenites.|
15666|Punkerri Sandstone|22922|6|Mentioned|33 fig 2|||||||||
15666|Punkerri Sandstone|23282|1|Redefined|p67||Neoproterozoic|Equivalent to Pound Subgroup in the Adelaide Fold Belt. Original Punkerri Sandstone by Thomson (1969), then redefined as Punkerri Beds by Major (1974), now redefined as Punkerri Sandstone. Of Ungoolya Group, Officer Basin. Age: Neoprot - latest Marinoan.||||||30-SEP-08
15666|Punkerri Sandstone|23818|6|Mentioned|p78|||Contains Ediacara sea pen fossil types.||||||
15666|Punkerri Sandstone|24067|5|Briefly described|p249 Fig.2|Adelaidean|Adelaidean|Geological Province: Officer Basin.||||||
15666|Punkerri Sandstone|24112|5|Briefly described|p254 Fig.2|Neoproterozoic|Neoproterozoic|Of the Ungoolya Group. Geological Province: Officer Basin||||||
15666|Punkerri Sandstone|30218|6|Mentioned|p404|||||||||
15666|Punkerri Sandstone|30807|6|Mentioned|p102|||Suggested map symbol||||||
15666|Punkerri Sandstone|30923|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
15666|Punkerri Sandstone|31965|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
15666|Punkerri Sandstone|31969|6|Mentioned|p9|||||||||
15666|Punkerri Sandstone|31971|6|Mentioned|p6|||See also P8||||||
15666|Punkerri Sandstone|31973|6|Mentioned|p5|||Now Punkerri Beds. Top & bottom not exposed.||||||
15666|Punkerri Sandstone|33655|5|Briefly described|p100|||||||||
15666|Punkerri Sandstone|34535|6|Mentioned|p78|||||||||
15666|Punkerri Sandstone|39352|6|Mentioned|Map legend|Adelaidean|Adelaidean|Marinoan||||||
15666|Punkerri Sandstone|42661|6|Mentioned|p130|||||||||
15666|Punkerri Sandstone|43743|6|Mentioned|Fig.2,p33||Neoproterozoic|||||||
15666|Punkerri Sandstone|44133|5|Briefly described|p39|Neoproterozoic|Neoproterozoic|Unconformably underlies Wirrildar beds, Kulyong Volcanics.||||||
15666|Punkerri Sandstone|60953|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Shallow marine sandstone and siltstone.||||||27-APR-05
15666|Punkerri Sandstone|61108|5|Briefly described|map legend|Adelaidean|Adelaidean|Shallow marine sandstone and siltstone.||||||06-JUN-05
15666|Punkerri Sandstone|61732|4|Described|p58 Fig. 22, p67|Ediacaran|Ediacaran|Of Ungoolya Group. Previously known as "Punkerri beds" or "Punkerri Fm". Redefined by Morton (1997). Max. thickness: >1200m. In type section. Geol.Prov: Officer Basin. See also p145 Fig. 51.G106.||||||07-FEB-11
15666|Punkerri Sandstone|62453|4|Described|p14, 50|Ediacaran|Ediacaran|Quartzite, sandstone, siltstone, minor conglomerate and carbonate. Overlies disconformably: Wright Hill Formation. Underlies; Wirrildar beds.||||||
15666|Punkerri Sandstone|64580|4|Described|map legend||Neoproterozoic|Quartz sandstone, feldspathic sandstone, and siltstone; minor conglomerate.||||||09-DEC-08
15666|Punkerri Sandstone|65416|6|Mentioned|p144.|Late Proterozoic|Late Proterozoic|||||Is overlain by Wirrildar beds.||
15666|Punkerri Sandstone|67536|6|Mentioned|Map Legend|||One of several Formations mapped collectively as N2.|||||Dominantly marine shale, siltstone, sandstone and limestone.|
15666|Punkerri Sandstone|67921|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Shown only in section and grouped with Ungoolya Group (Rodda beds), Karlaya Limestone, Wright Hill beds. Group description: Marine sandstone, grey indurated mudstone and limestone.||||Said to be equivalent to Wilpena Group||
15666|Punkerri Sandstone|69153|6|Mentioned|500k_geologyp08_lut.csv||Neoproterozoic||||||Quartz sandstone, feldspathic sandstone, and siltstone; minor conglomerate|
15666|Punkerri Sandstone|70634|4|Described|500k_geolgyp08_lut.csv|Neoproterozoic|Neoproterozoic||||||Quartz sandstone, feldspathic sandstone, and siltstone; minor conglomerate.|
15666|Punkerri Sandstone|70790|6|Mentioned|p271|||||||Equivalent to Bonney Sandstone.||
15666|Punkerri Sandstone|70793|4|Described|500k_interpgeop14_lut.csv|Ediacaran|Ediacaran|Of Officer Basin (Phase 1), Centralian Superbasin. Events: Areyonga Movement; Delamarian Orogeny (520-505 Ma); Petermann Orogeny (580-520 Ma).|635-541 Ma (biostrat; inferred)||||Sandstone, reddish brown, flaggy, micaceous to feldspathic, and lesser siltstone|
15666|Punkerri Sandstone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||siltstone, sandstone|
15666|Punkerri Sandstone|71268|5|Briefly described|1m_geologyp12_lut.csv|||||Unit of Ungoolya Group.|||Lower purple, red-brown flaggy sandstone; upper red, white feldspathic and quartzose sandstone, interbedded siltstone|
15666|Punkerri Sandstone|72034|5|Briefly described|500k_interpgeop16_lut|Ediacaran|Ediacaran|Officer Basin (Phase 1).|||||Sandstone, reddish brown, flaggy, micaceous to feldspathic, and lesser siltstone.|
15666|Punkerri Sandstone|72478|6|Mentioned|p8|Marinoan|Marinoan|Officer Basin.|c. 570 Ma-545 Ma|Ungoolya Group||Unconformably overlies Munyarai Formation. Unconformably overlain by the Relief Sandstone.||24-MAR-21
15666|Punkerri Sandstone|73100|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Subsurface.||||Equivalent to Wilpena Group.||
15666|Punkerri Sandstone|73109|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Subsurface.||||Equivalent to Wilpena Group.||
15666|Punkerri Sandstone|73111|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Subsurface.||||Equivalent to Wilpena Group.||
15684|Purni Formation|13516|6|Mentioned|p147, fig 5|Early Permian|Early Permian|From Pedirka Basin||||||
15684|Purni Formation|22883|6|Mentioned|P29|Early Permian|Late Carboniferous|Underlying unit is Crown Point Formation.||||||27-NOV-06
15684|Purni Formation|23982|6|Mentioned|p96 Appendix 13|||Geological Province: Great Artesian Basin.||||||
15684|Purni Formation|24204|5|Briefly described|p262, 263 Fig.4, p266 Fig.7|Early Permian|Early Permian|Geological Province: Pedirka Basin.||||||
15684|Purni Formation|30514|6|Mentioned|p100|||Permian age||||||
15684|Purni Formation|30540|6|Mentioned|p67|||Similar to Patchawarra Formation of Cooper Basin||||||
15684|Purni Formation|30544|5|Briefly described|p52|||In the Pedirka Basin.||||||27-NOV-06
15684|Purni Formation|30825|6|Mentioned|p37|||||||||
15684|Purni Formation|33523|6|Mentioned|Fig.13|||||||||
15684|Purni Formation|33525|6|Mentioned|p5|||||||||
15684|Purni Formation|33824|6|Mentioned|p7|||||||||
15684|Purni Formation|33832|5|Briefly described|p7|||Stratigraphy||||||
15684|Purni Formation|33844|3|Fully described|p36|||||||||
15684|Purni Formation|33971|4|Described|p33|||||||||
15684|Purni Formation|33976|2|Defined|p5|Permian|Permian|||||||
15684|Purni Formation|35845|6|Mentioned|Fig.25|||||||||
15684|Purni Formation|36733|6|Mentioned|p14|||||||||
15684|Purni Formation|36922|6|Mentioned|p188|||||||||
15684|Purni Formation|37065|6|Mentioned|p30|||||||||
15684|Purni Formation|37776|6|Mentioned|Fig.2|||||||||
15684|Purni Formation|37855|6|Mentioned|Fig.2|||||||||
15684|Purni Formation|37917|4|Described|p470|||||||||
15684|Purni Formation|38958|5|Briefly described|p491|||||||||
15684|Purni Formation|39265|6|Mentioned|Fig. 3|||||||||
15684|Purni Formation|40637|6|Mentioned|Fig.2|||||||||
15684|Purni Formation|40910|6|Mentioned|p14|||||||||
15684|Purni Formation|40911|6|Mentioned|Map legend|Permian|Carboniferous|||||||
15684|Purni Formation|40925|6|Mentioned|Map legend|Permian|Carboniferous|Carboniferous to Permian||||||
15684|Purni Formation|40926|3|Fully described|p13|||||||||
15684|Purni Formation|41063|6|Mentioned|p40|||||||||
15684|Purni Formation|41183|6|Mentioned|p314|||||||||
15684|Purni Formation|41270|6|Mentioned|p279|||||||||
15684|Purni Formation|41491|6|Mentioned|p180|||||||||
15684|Purni Formation|41689|6|Mentioned|Table 1|||||||||
15684|Purni Formation|42463|6|Mentioned|Fig.4 P171|||||||||
15684|Purni Formation|42504|5|Briefly described|p81|||||||||
15684|Purni Formation|42547|4|Described|p82|||||||||
15684|Purni Formation|42746|5|Briefly described|p6, Fig.2 p4|||In the Pedirka Basin.||||||27-NOV-06
15684|Purni Formation|43052|5|Briefly described|Table 2.1|||||||||
15684|Purni Formation|44133|5|Briefly described|p65 Fig. 8.3, 90|Permain|Permain|Geological Province: Pedirka Basin. Probably conformably overlies Crown Point Formation.||||||
15684|Purni Formation|61250|5|Briefly described|p43|Permian|Early Permian|Includes a glacigene sandstone at base. Important oil source rock - contains petroleum systems. Geological Province: Perdika Basin. Correlates with Patchawarra Formation and Tirrawarra Sandstone.||||||18-AUG-05
15684|Purni Formation|62376|5|Briefly described|p84|Early Permain|Early Permian|Geological Province: Pedirka Basin.||||||09-FEB-10
15684|Purni Formation|62759|5|Briefly described|p1|Early Permian|Early Permian|Important oil source rock. Geological Province: Perdika/Eromanga Basins. Correlates with Patchewarra Formation in the Cooper Basin.||||||05-FEB-08
15684|Purni Formation|64232|5|Briefly described|p12|||Geological Province: Perdika Basin. Sub-bituminous coal seams are well-developed at suitable depths for CSM exploration in Mount Hammersley area.||||||24-JUL-08
15684|Purni Formation|64778|6|Mentioned|p13, 15-21, 23, 28, 33|Permian|Permian|Pedirka Basin. Thermal history summarised. Max. palaeotemperature analysis summary. Potential hydrocarbon source rock.|285-270 Ma.|||||
15684|Purni Formation|65238|5|Briefly described|p3, p5 Fig. 6, p7 Fig. 8|Permian|Permian|Conformably overlies Crown Point Fm; overlain by Poolowanna Fm. Geol.province: Pedirka Basin. Lacustrine, meander, fluvial-swamp deposits. Lithological details of three unnamed members included on p8 - total max.thickness being 350m. See also p14 Fig. 17||||||09-APR-13
15684|Purni Formation|65489|5|Briefly described|p13, p17, p55-61, p63-64, p91, p137-139|Permian|Permian|See also p143, p151. Pedirka Basin. 350m thick. Contains very thick coal sequences, and a well, drilled for coal bed methane, has been successful (CBM93001). Fair to exellent hydrocarbon source and reservoir potential.||||Overlies Crown Point Formation. Is correlated with Patchawarra Formation (Cooper Basin).|Alternating shale, coal and siltstones of lacustrine, swamp and floodplain deposition; also point-bar and other channel-derived sands.|
15684|Purni Formation|69418|5|Briefly described|p3:34|Permian|Permian|Pedirka Basin. Contains coal seams over 30m thick, extending over 70km along strike.||||||12-JUL-16
15684|Purni Formation|69454|4|Described|p38:3-4, 6-8, 10-15|Guadalupian|Asselian|Youngs (1975). Widespread in W Pedirka Basin. 564.3m thick in Blamore-1. Four sub-units ("facies suites") are described in some detail; the authors suggest possibly elevating the Formation to Group status and defining the subdivisions as Formations (depending on further study). Glaciofluvial outwash, flood plain/overbank, fluvial and paludal depositional environments. Considered to be lateral equivalent of the Patchawarra Formation and younger Gidgealpa Group units (Cooper Basin). Hosts significant coal-bearing intervals (detailed) with potential also for coal gasification or coal-to-liquid processing, as well as fair to good petroleum source potential. Sandstones have some reservoir potential, with intra-formational shale seals, while basal shale could seal underlying Tirrawarra Sandstone reservoirs.||||Conformably overlies Tirrawarra Sandstone or Crown Point Formation. Is overlain unconformably by Walkandi, Peera Peera Formations. Lateral equivalent of Stuart Range and Mount Toondina Formations.|Sandstone (locally pyritic), siltstone, shale, carbonaceous shale, coal, minor conglomerate.|12-JUL-16
15684|Purni Formation|69457|6|Mentioned|p41:5 Fig.41.4; 41:16-17|Permian|Permian|Fair to good source rocks.||||||12-JUL-16
15684|Purni Formation|69673|5|Briefly described|p151, p152, p159, p160, p161, p162, p164|Permian|Permian|greater than 550m thick. Contains five unnamed units. Source rock potential.||||Conformably overlies Crown Point Formation, overlies Tirrawarra Sandstone, unconformably overlain by Walkandi Formation, Peera Peera Formation, Algebuckina Sandstone|Sandstone, siltstone, shale, coal and minor conglomerate.|
15684|Purni Formation|69946|4|Described|p5, p7-8, p36, p44-45, p48-51|Artinskian|Asselian|Pedirka Basin. Defined by Youngs (1975) after informal references by Jacque (1966). Type section is the interval 1417 - 1698m in Purni 1. Up to 350m thick.||||Disconformably overlies Crown Point and Mount Toondina Formations.|Basal interbeds of grey shale and fine- to medium-grained sandstone, minor conglomerate and coal stringers; cross-bedded sandstone with interbeds of siltstone, shale and minor coal; silty sandstone, carbonaceous shale interbeds, abundant coal seams.|
15684|Purni Formation|69948|6|Mentioned|Fig.4.18|||Pedirka Basin.||||Unconformably overlies Mount Toondina, Stuart Range and Crown Point Formations. Is overlain unconformably by Algebuckina Sandstone and (locally) Walkandi, Peera Peera and Poolowanna Formations.||
15684|Purni Formation|71342|4|Described|Ch4 p25, Ch5 p5, Ch5 p7-p8|Early Permian|Early Permian|Pedirka Basin. Formally defined by Youngs (1975) following informal references by Jacque (1966) in the Mokari 1 well completion report. A type section in Purni 1 is mentioned. This unit is subdivided into three members at the type section, these are described further in Ch5 p7. A maximum thickness of 350m is recorded in Mokari 1. See also  Ch5 p30, Ch5 p36, Ch5 p44-p45, Ch5 p49-p51, Ch8 p28, Ch9 p16, Ch9 p18, Ch9 p20-p21, Ch11 p6, Ch14 p5-p7.||||Disconformably overlies the Crown Point Formation. Unconformably overlies the Finke Group.|Interbedded grey shale and fine to medium-grained sandstone with minor conglomerate and coal stringers.|
15684|Purni Formation|72476|6|Mentioned|p26, p36 Fig.9|Permian|Carboniferous|Perdika Basin. Time-temperature thermal history diagram.||||||
15684|Purni Formation|73281|6|Mentioned|p1, Appendix (DIP)|Permian|Permian|Pedirka Basin. Coal-rich. Petroleum source rocks. Data included in digital information package (DIP) 034. See DIP034_Petroleumdata.xlsx and DIP034_Welldata.xlsx. Also written as Purni Formation, lower.||||||
15689|Pussy Cat Group|30385|6|Mentioned|p8|||||||||
15689|Pussy Cat Group|30388|4|Described|Table 1|||Middle Proterozoic age. Equivalent? to Tollu Group.||||||09-DEC-08
15689|Pussy Cat Group|30390|4|Described|p49|||See also P50||||||
15689|Pussy Cat Group|30878|6|Mentioned|p51|||Precambrian. Stratigraphic table||||||
15689|Pussy Cat Group|30944|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
15689|Pussy Cat Group|30946|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Part of Bentley Supergroup||||||
15689|Pussy Cat Group|30947|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
15689|Pussy Cat Group|36551|6|Mentioned|Table 31|||||||||
15689|Pussy Cat Group|36701|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
15689|Pussy Cat Group|36886|4|Described|p196|||||||||
15689|Pussy Cat Group|37707|6|Mentioned|p24|||||||||
15689|Pussy Cat Group|44139|5|Briefly described|p284, Table 3-16|||Of Bentley Supergroup. ~300m. Basalt, minor rhyolite. May be equivalent to Tollu Group.|| ||||10-SEP-12
15689|Pussy Cat Group|45149|5|Briefly described|p19|||||||||
15689|Pussy Cat Group|50607|6|Mentioned|p3.2|||Geological Province: Musgrave Block.||||||
15689|Pussy Cat Group|61524|5|Briefly described|p17 Fig.1|Mesoproterozoic|Mesoproterozoic|Volcanics. Geological Province: Musgrave Province.||||||
15689|Pussy Cat Group|61864|6|Mentioned|p18 fig 4|||Volcanics.||||||
15689|Pussy Cat Group|62453|6|Mentioned|p15|||Of the Bentley Supergroup.||||||
15689|Pussy Cat Group|63866|5|Briefly described|p202|||Musgrave Province.||Bentley Supergroup||||
15689|Pussy Cat Group|64580|4|Described|map legend||Mesoproterozoic|Of Bentley Supergroup. Rhyolite, dacite, ignimbrite, basalt, volcaniclastic sedimentary rock, sandstone, and conglomerate.||||||09-DEC-08
15689|Pussy Cat Group|65256|6|Mentioned|p14, p30|||Lateral equivalent of the Tollu Group; may be equivalent to Tjuninanta Formation (Tjauwata Group). Includes Glyde Formation.||||||
15689|Pussy Cat Group|67244|5|Briefly described|Map legend.|||Bentley Basin. Shown only in the Interpreted Bedrock Geology section of the map sheet.|||Includes Glyde Formation.|||11-APR-12
15689|Pussy Cat Group|67372|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Bentley Basin.||Unit in Bentley Supergroup.|Includes Glyde Formation.|||
15689|Pussy Cat Group|67375|4|Described|p7, pp8-9 Fig.5, p38 Table 1, pp46-47.|Mesoproterozoic|Mesoproterozoic|Talbot Sub-basin, Musgrave Region. May be laterally equivalent to Tollu Group.|1071-1065 Ma.|Unit in Bentley Supergroup.|Includes Kathleen Ignimbrite and Glyde Formation.|Overlies Scamp rhyolite (informal name). Is overlain by Cassidy Group.|Metabasalts and intercalated metasedimentary rocks.|
15689|Pussy Cat Group|67553|5|Briefly described|p8,11,17,40-42,48-50,59,94,97-98|Stenian|Stenian|Geological province: Musgrave Province, North Australian Craton. Of Blackstone Sub-basin, Bentley Sub-basin. [Also misspelt as Pussycat Group on p98]. Affected by an episode of syn- to post-depositional folding. Outcropping portions up to 3000m thick, however full thickness is uncertain.|1071-1065 Ma|Unit of Bentley Supergroup.|Includes Glyde Formation and Kathleen Ignimbrite.|Conformably overlain by Cassidy Group/Wururu Rhyolite.||06-AUG-19
15689|Pussy Cat Group|68995|4|Described|p3-4, p7-9, p15, p24, p27 Tb.2, p45-46|Stenian|Stenian|Talbot Sub-basin. Age based on the Giles Event which occurred as this unit was deposited. At least 3500m thick based on outcrop; 2100m of this is basaltic lava flows.|c. 1085-1040 Ma|Bentley Supergroup|Glyde Formation, Kathleen Ignimbrite|Overlies the Mount Waugh rhyolite (apparently conformably) and the Kaarnka Group. (Maybe unconformably) overlain by the Cassidy Group.|Bimodal volcanic rocks with less common sedimentary rocks that shallowly dip.|
15689|Pussy Cat Group|68996|5|Briefly described|p5, 7, p32-39, p47, 50, 65|Mesoproterozoic|Mesoproterozoic||1071 +/- 5 Ma (SHRIMP)|Bentley Supergroup|Includes Kathleen Ignimbrite, Glyde Formation|||
15689|Pussy Cat Group|69003|5|Briefly described|p37, p51-52|Mesoproterozoic|Mesoproterozoic|Talbot Sub-basin, west Musgrave Province.|1071 +/- 5 Ma - 1065 +/- 5 Ma.|Bentley Supergroup.|Glyde Formation, Kathleen Ignimbrite.|Is overlain (probably unconformably) by Cassidy Group.||
15689|Pussy Cat Group|69009|5|Briefly described|Map Legend|Stenian|Stenian|Bentley Basin.|1071-1047 Ma|Of the Bentley Supergroup.|Includes Kathleen Ignimbrite.||Comprises quartz-feldspar-porphyritic rhyolite; volcaniclasitc rhyolite; diamictite; sandstone and siltstone to mudstone; rhyolite.|
15689|Pussy Cat Group|69091|4|Described|p30 Fig.3.5, p41 Fig.3.8, see comments|||Talbot Sub-basin, Musgrave Province. Bimodal volcanic rocks and less common sedimentary units dip shallowly (less than 30 degrees) to south and southwest, and form continuous packages that can be traced for over 100 km. See also p52 Fig.4.1, p54 Fig.4.2, p59 Fig.4.6, p71 Fig.4.14, p75, p81 Fig.4.17, p106 Fig.5.7a, p107 Fig.5.8a, p108 Fig.5.9, p109 Fig.5.10, p115 Fig.5.14, p117 Fig.5.15, p119 Fig.5.16, p131 Fig.6.1, p133, p144, p174 Fig.9.5, p177 Fig.9.6, p200 Fig.10.2.||Bentley Supergroup|Kathleen Ignimbrite, Glyde Formation|Overlies Mount Palgrave and Kaarnka Groups; is overlain by Cassidy Group.|Continuous packages of bimodal volcanic rocks and less common sedimentary units.|
15689|Pussy Cat Group|69153|5|Briefly described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Bentley Basin, Paterson Orogen||Bentley Supergroup|Glyde Formation, Kathleen Ignimbrite||Sedimentary siliciclastic (sandstone, siltstone, mudstone; rare conglomerate of basalt, rhyolite and granite cobbles), evaporites, diamictite; interbedded basalt, basaltic andesite; porphyritic quartz-feldspar rhyolite; subvolcanic intrusion - mafic|
15689|Pussy Cat Group|69655|5|Briefly described|p3, p6|Stenian|Stenian|Musgrave Region.|c. 1090-1040 Ma|Bentley Supergroup||||
15689|Pussy Cat Group|69729|5|Briefly described|p66 Fig.1, p68, p70, p80, p82|||Talbot Sub-basin, Musgrave Province.||Bentley Supergroup.|Glyde Formation, Kathleen Ignimbrite.|Overlies the Mount Palgrave Group. Is overlain by the Cassidy Group.||
15689|Pussy Cat Group|70095|5|Briefly described|p16-19|||Geological province: Musgrave Province. Of Talbot Sub-basin, Bentley Basin. [Name is hyphenated on p16]. Thickness of rhyolitic package: 0.9km; thickness of basaltic package: 2.1km. Strike length: over 200km, over multiple eruptive events. See p19 Table 2 for U-Pb zircon data. See p21 Table 3 for SIMS oxygen isotope data.||Unit of Bentley Supergroup.|Includes Kathleen Ignimbrite and Kaarnka Group.|Overlain by Cassidy Group/Wururu Rhyolite. Underlain by Mount Palgrave Group/Mount Waugh rhyolite.||
15689|Pussy Cat Group|70134|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Bentley Basin.|1071-1047 Ma.|Bentley Supergroup.|Glyde Formation.|Overlies Mount Palgrave Group. Is overlain by Cassidy Group.||
15689|Pussy Cat Group|70137|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Bentley Basin.||Bentley Supergroup.|Glyde Formation.||Rhyolite, vesicular and amygdaloidal basalt, basaltic andesite, andesite, medium- to fine-grained siliciclastic rocks, rare calc-silicate rocks, evaporite horizons and microbialites.|
15689|Pussy Cat Group|70634|4|Described|100k_geologyp_lut,csv|Mesoproterozoic|Mesoproterozoic||1049 Ma - 1077 Ma (Inferred)|Bentley Supergroup|Includes Kathleen Ignimbrite||Vesicular and amygdaloidal basalt and minor basaltic andesite with minor siliciclastic interbeds. Porphyritic quartz-feldspar rhyolite with rounded quartz and alkali feldspar phenocrysts; fine grained micrographic to felsitic groundmass.|
15689|Pussy Cat Group|70793|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Geological province: Paterson Orogen, Musgrave Province. Of Bentley Basin. Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma); Giles Event (1085-1040 Ma). See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop14_lut.csv, 100k_interpgeol_lut.csv, 500k_interpgeop_lut.csv, 100k_geologyl_lut.csv, 250k_interpgeol_lut.csv, 2_5m_interpgeop15_lut.csv.|1077-1047 Ma (inferred)|Unit of Bentley Supergroup.|Includes Glyde Formation and Kathleen Ignimbrite.||Vesicular and amygdaloidal basalt, and minor basaltic andesite; locally plagioclase porphyritic; quartz-feldpsar-porphyritic rhyolite, interbedded sandstone and medium- to fine-grained siliciclastic rocks.|
15689|Pussy Cat Group|70826|6|Mentioned|p5 tbl 2, p10|Mesoproterozoic|Mesoproterozoic|Bentley Basin. Shown as Pussycat Group p10.||Bentley Supergroup||||20-APR-20
15689|Pussy Cat Group|70831|5|Briefly described|p3, p5|||Musgrave Province.||Bentley Supergroup||||
15689|Pussy Cat Group|71170|5|Briefly described|p5-p6|||Talbot Sub-basin. Emplaced during the Giles Event.||Bentley Supergroup||||
15689|Pussy Cat Group|71210|6|Mentioned|p5|||Talbot Sub-basin.||||||
15689|Pussy Cat Group|71211|4|Described|i-iii, vii, ix-xi, xiii, p1|Mesoproterozoic|Mesoproterozoic|Talbot Sub-basin. Magmas of this group were evolved, anhydrous, metaluminous A-types that were enriched in REE. On the basis of geochemistry this Group is interpreted to have been formed primarily by mantle derived magmas. See also p6 fig 1.3, p7 fig 1.4, p11, p13  p24 fig 2.1, p25, p26, p63, p81-p84, p86, p88-p89 fig 3.3, p94, p96, p99 fig 3.7, p102-p108, p110, p112, p113, p115-p117, p119-p120, p135, p136 fig 4.1, p208-p210, p212, p215-p216, p234, p265-p266.|1085-1040 Ma|Bentley Supergroup|Includes the Rowland Suite, Kathleen Ignimbrite, Glyde Formation and (the Cleghorne Formation).|Conformably overlies the Mount Palgrave and Kaarnka Groups. Overlain by the Cassidy and Mission Groups.|Rhyolitic magmas.|01-SEP-17
15689|Pussy Cat Group|71268|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Geological Province: Paterson Orogen. Of Bentley Basin. Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma); Giles Event (1085-1040 Ma). See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 1m_geologyp12_lut.csv, 500k_interpgeop16_lut.csv, 100k_interpgeol_lut.csv, 100k_geologyl_lut.csv, 250k_interpgeol_lut.csv, 2_5m_interpgeop15_lut.csv.||Unit of Bentley Supergroup.|Includes Glyde Formation, Kathleen Ignimbrite.||Vesicular and amygdaloidal basalt, and minor basaltic andesite; locally plagioclase porphyritic; epidotized; quartz-feldspar-porphyritic rhyolite; diamictite, conglomerate, interbedded sandstone, siltstone and mudstone.|
15689|Pussy Cat Group|72034|5|Briefly described|500k_interpgeop16_lut|Mesoproterozoic|Mesoproterozoic|Bentley Basin. Four informal sub-units specified [Unclear how these might relate to the 4 named units that form the Pussy Cat Group].|||Includes Glyde Formation, Kathleen Ignimbrite.||Porphyritic rhyolite; subvolcanic. Matrix- to clast-supported conglom.; mainly basalt cobbles; interbedded w med. to fine siliciclastics. Diamictite; subrounded/angular mafic/felsic volc. clasts. Med. to fine siliciclastics, interbedded w basalt.|
15689|Pussy Cat Group|72094|4|Described|p3 Fig 2, p4, 7, 13|Stenian|Stenian|Talbot Sub-basin, Bentley Basin. Intruded by Warakurna Supersuite intrusions with U-Pb 1071+\-5, 1063+\-8 and 1049+\-8 Ma zircon ages (Smithies et al., 2013b).||Unit of Bentley Supergroup.||Underlain, and intruded by fine- to medium-grained intrusions of the Warakurna Supersuite.|Vesicular and amygdaloidal basalt, locally with voluminous volcaniclastic rhyolite and intercalated fine- to coarse-grained volcaniclastic and siliciclastic rocks.|
15689|Pussy Cat Group|72443|5|Briefly described|p737-740, p742, p753|||Talbot Sub-basin.|1081 +/- 9 to 1070 +/- 11 Ma (SHRIMP U-Pb)|Bentley Supergroup|Includes the Glyde Formation and the Kathleen Ignimbrite.|Overlies the Mount Palgrave Group. Overlain by the Cassidy Group.|Dominantly ignimbrite and overlying amygdaloidal basaltic lavas and interlayered volcaniclastic sedimentary rocks.|
15689|Pussy Cat Group|73437|6|Mentioned|p151|Mesoproterozoic|Mesoproterozoic|Bentley Basin, Talbot Sub-basin.||Bentley Supergroup||||
15734|Quartoo Sand Member|30251|6|Mentioned|p3|||Table on P3.||||||
15734|Quartoo Sand Member|33330|2|Defined|p156|late Eocene|late Eocene|||||||
15734|Quartoo Sand Member|35689|6|Mentioned|Fig.33|||Stratigraphic correlation, St.Vincent Basin.||||||
15734|Quartoo Sand Member|41513|6|Mentioned|p45|||||||||
15734|Quartoo Sand Member|44133|5|Briefly described|p165 Fig. 10.11|Late Eocene|Middle Eocene|Of the Muloowurtie Sand Member. Geological Province: Saint Vincent Basin.||||||
15734|Quartoo Sand Member|60958|5|Briefly described|Map Legend|Eocene|Eocene|Of the Muloowurtie Formation. Geological Province: Saint Vincent Basin.  Medium to coarse-grained cross-bedded esturine sandstone and grit layers.||||||14-APR-05
15734|Quartoo Sand Member|61121|5|Briefly described|Map legend|Eocene|Eocene|Of the Muloowurtie Formation. Medium- to coarse-grained, cross-bedded etsuarine sandstone and grit layers. Geological Province: St. Vincent Basin.||||||06-JUN-05
15734|Quartoo Sand Member|65375|5|Briefly described|pp34-35.|Eocene|Eocene|Lens up to 3m thick, dividing the Muloowurtie Formation into lower and upper parts. Possibly deposited in nearshore submarine channel or estuary.||Of Muloowurtie Formation|||A lens of variegated quartzitic, medium- to coarse-grained and granule sandstone.|
15734|Quartoo Sand Member|67462|5|Briefly described|Map legend.|Eocene|Eocene|Western Saint Vincent Basin.||Unit in Muloowurtie Formation.||||
15734|Quartoo Sand Member|68715|6|Mentioned|p31 Fig.5|Bartonian|Lutetian|St Vincent Basin.||||||
15734|Quartoo Sand Member|70382|4|Described|p27, p28-29, p30, p31, p34, p35|Eocene|Eocene|St Vincent Basin. Maximum thickness 6.4 m. Pb/Pb and Pb/U detrital zircon dating yielded zircon ages ranging from 3381+\-22 Ma to 256+\-4 Ma, from various sources. 582-485 Ma zircons were likely derived from reworking of Permian sediments, and transported from the south. 1600 Ma zircons could be from the proximal Hiltaba Suite or Arthurton Grante from the Yorke Peninsula. 1846 Ma zircons from the Donington Suite also suggest zircon provenance from the south from the Yorke Peninsula. Mesoarchean zircons however, may have been derived from a NW source e.g. Middleback Subgroup of the northern Eyre Peninsula, or recycling from another sedimentary source in the region.||Unit of the Muloowurtie Formation.||Upper section of the Muloowurtie Formation.|~3 m of upwards coarsening, red-brown oxidised sands overlain by ~2 m of silicified, cross-bedded sands. Medium to coarse grained, well sorted, with a very low content of clay and silt. Near-shore channel or estuarine-style sediments.|
15792|Radium Ridge Breccia|41258|2|Defined|p22|Silurian|Late Ordovician|Formerly Radium Ridge Beds.||||||16-FEB-09
15841|Ranmoor Member|23430|4|Described|p524 Table 14.7|||Of Wallumbilla Formation. Eromanga Basin Province.||||||
15841|Ranmoor Member|23982|5|Briefly described|p58 Fig.18|||Of Wallumbilla Formation. Geological Province: Eromanga Basin.||||||
15841|Ranmoor Member|24092|5|Briefly described|p8 Fig.3|||Of Wallumbilla Formation. Geological Province: Eromanga Basin.||||||
15841|Ranmoor Member|30020|6|Mentioned|p33|||||||||
15841|Ranmoor Member|30024|6|Mentioned|p332|||||||||
15841|Ranmoor Member|30042|6|Mentioned|p5|||Tambo faunas correlation.||||||
15841|Ranmoor Member|30443|6|Mentioned|p14|||Albian age||||||
15841|Ranmoor Member|31208|6|Mentioned|p48|||||||||
15841|Ranmoor Member|32314|6|Mentioned|Fig. 4|||||||||
15841|Ranmoor Member|33016|6|Mentioned|p1|||On table||||||
15841|Ranmoor Member|33017|6|Mentioned|p6|||||||||
15841|Ranmoor Member|33086|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
15841|Ranmoor Member|33165|6|Mentioned|Chart|||Correlation chart only||||||
15841|Ranmoor Member|33175|5|Briefly described|p280|||||||||
15841|Ranmoor Member|33182|6|Mentioned|Table 1|||L.Cret.||||||
15841|Ranmoor Member|33368|6|Mentioned|p25|||Strat. table.||||||
15841|Ranmoor Member|33414|6|Mentioned|p212,Tb.||Cretaceous|Part of Wallumbilla Formation.||||||
15841|Ranmoor Member|33638|5|Briefly described|Table 1|||||||||
15841|Ranmoor Member|33640|6|Mentioned|p12|||||||||
15841|Ranmoor Member|33642|6|Mentioned|144,147-8,Tb.1,Fig.2|||Refers Vine & Day(1965). Lower part-Lower Albian fauna, upper part has possible Middle Albian fossils.||||||
15841|Ranmoor Member|33643|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
15841|Ranmoor Member|33644|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
15841|Ranmoor Member|33648|6|Mentioned|p21|||Strat.||||||
15841|Ranmoor Member|34091|5|Briefly described|Table 1|||L.Cret||||||
15841|Ranmoor Member|35239|6|Mentioned|p265|||||||||
15841|Ranmoor Member|35560|6|Mentioned|p291|||||||||
15841|Ranmoor Member|35793|6|Mentioned|Fig.3|||||||||
15841|Ranmoor Member|35811|6|Mentioned|p556|||Exploration carried out.||||||
15841|Ranmoor Member|35855|6|Mentioned|Fig.2|||Early Cretaceous lithostratigraphy.||||||
15841|Ranmoor Member|36552|6|Mentioned|p61|||||||||
15841|Ranmoor Member|36571|6|Mentioned|Table 4|||||||||
15841|Ranmoor Member|38199|6|Mentioned|p428|||See also P429.||||||
15841|Ranmoor Member|38814|6|Mentioned|Table 1|||||||||
15841|Ranmoor Member|39211|5|Briefly described|Fig.3|||See also Figs 9,11,12 etc.Correlation||||||
15841|Ranmoor Member|40801|6|Mentioned|p46|||||||||
15841|Ranmoor Member|40926|6|Mentioned|Table 2|||||||||
15841|Ranmoor Member|41086|3|Fully described|Fig.3|||||||||
15841|Ranmoor Member|41088|6|Mentioned|p141|||||||||
15841|Ranmoor Member|41266|6|Mentioned|Fig.3|||||||||
15841|Ranmoor Member|44082|6|Mentioned|p10,18-20,Tb.p34||Albian|(Early Albian) Part of Wallumbilla Formation. Mentioned with respect to Qld Cretaceous fossils which are either of stratigraphic significance or are illustrative of the occurrence of a particular group.||||||
15841|Ranmoor Member|44087|14|Not recorded|p4,opp.7|||||||||
15841|Ranmoor Member|44089|14|Not recorded|Tb.1,p4||Early Cretaceous|(Wilgunya Formation)||||||
15841|Ranmoor Member|44346|14|Not recorded|p4,opp.p5||Aptian|?Aptian||||||
15841|Ranmoor Member|44352|14|Not recorded|Map Legend||Early Cretaceous|||||||
15841|Ranmoor Member|44373|14|Not recorded|p20|||Map only.||||||
15841|Ranmoor Member|44374|14|Not recorded|p12|||Albian in lower part, highly mudstone sequence, with carbonaceous interval, equivalent to non-marine Coreena Member.||||||
15841|Ranmoor Member|44406|14|Not recorded|p4,opp.p6|||Member of Wilgunya Formation.||||||
15841|Ranmoor Member|44408|14|Not recorded|p4,opp.p6||Aptian|||||||
15841|Ranmoor Member|44414|14|Not recorded|p110-112,114||Cretaceous|Correlated with Coreena Member.||||||
15841|Ranmoor Member|44417|2|Defined|p416,418-420||Albian|(Early Albian)||||||
15841|Ranmoor Member|44915|14|Not recorded|p18||Early Cretaceous|Ref. to Vine and Day 1965.||||||
15841|Ranmoor Member|45132|6|Mentioned|p11|||||||||
15841|Ranmoor Member|45145|6|Mentioned|p61|||||||||
15841|Ranmoor Member|46791|6|Mentioned|p44|||||||||
15841|Ranmoor Member|46937|6|Mentioned|Fig.10|||||||||
15841|Ranmoor Member|48908|14|Not recorded|Tb.1||Early Cretaceous|||||||
15841|Ranmoor Member|48920|6|Mentioned|p60|||See also Table 8. Refers Vine & Day (1965)||||||
15841|Ranmoor Member|49010|6|Mentioned|Fig.4|||Eromanga Basin||||||
15841|Ranmoor Member|49011|6|Mentioned|Fig.3|||Eromanga Basin||||||
15841|Ranmoor Member|60331|5|Briefly described|p34 Fig.3|Albian|Albian|Of Wallumbilla Formation. Overlies Jones Valley Member. Geological Province: Eromanga Basin.||||||
15841|Ranmoor Member|66529|6|Mentioned|p12 Fig.5|||||Unit in Wallumbilla Formation.||||
15841|Ranmoor Member|66623|6|Mentioned|p262.|||Equivalent to Coreena Member in NSW.||Unit in Rolling Downs Group in Queensland.||||
15841|Ranmoor Member|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map.|Cretaceous|Cretaceous|Eromanga/Carpentaria Basins.||Wallumbilla Formation.|||Mudstone, commonly carbonaceous, minor siltstone.|
15841|Ranmoor Member|67784|5|Briefly described|p25-26, p28 Tb.1, p29, p31-33|Albian|Aptian|60-95m thick. Northern Eromanga Basin.||Wallumbilla Formation||Paraconformably overlies Jones Valley Member. Is overlain by Toolebuc Formation.||08-FEB-18
15841|Ranmoor Member|68206|5|Briefly described|p32-33|Albian|Albian|NE Eromanga Basin.||Wallumbilla Formation.||Overlies Jones Valley Member. Is overlain by Toolebuc Formation.||
15841|Ranmoor Member|69457|6|Mentioned|p41:10|||Eromanga Basin. This and other Members of Wallumbilla Formation are not recognised in the NT.||Wallumbilla Formation.||||12-JUL-16
15841|Ranmoor Member|69594|4|Described|p522, p526, p528|Albian|Albian|Vine and Day (1965). Eromanga Basin. The type section is near Glendower Station, E of Hughenden. Crops out in a discontinuous band from Glendower to NW of Richmond. No equivalent units have been identified. Thickness generally 60-95m; may be up to 312m. Contains early Albian ammonite, bivalves and belemnites.||Wallumbilla Formation.||Conformably overlies Jones Valley Member.|Dominated by mudstone and siltstone, with minor labile sandstone.|
15841|Ranmoor Member|70860|6|Mentioned|p281|||Great Artesian Basin.||Wallumbilla Formation.||||
15841|Ranmoor Member|72297|5|Briefly described|p753|||Eromanga Basin.||Wallumbilla Formation.||Is overlain conformably by the Toolebuc Formation.|Blue shale.|
15841|Ranmoor Member|72298|5|Briefly described|p801|Cretaceous|Cretaceous|Eromanga Basin (SA,QLD).||Wallumbilla FZ.||Overlies Jones Valley Member. Is overlain by Toolebuc FZ.||
15851|Rathjen Gneiss|22634|6|Mentioned|p502,5|||||||||
15851|Rathjen Gneiss|22643|6|Mentioned|p186|||||||||
15851|Rathjen Gneiss|22726|6|Mentioned|p233|Late Cambrian|Neoproterozoic|||||||
15851|Rathjen Gneiss|22766|5|Briefly described|Fig.2 p561, p566|Early Cambrian|Early Cambrian|Age of unit 516+/-4 Ma. See also Fig.1 p560||||||
15851|Rathjen Gneiss|22945|6|Mentioned|p8|||Age - Cambro-Ordovician.  Mentioned under - Area C geology.||||||
15851|Rathjen Gneiss|23022|6|Mentioned|p1801|||||||||
15851|Rathjen Gneiss|23023|5|Briefly described|Fig1p1798,1799||Early Cambrian|Max Age: 516 (+/-) 4 Ma.||||||
15851|Rathjen Gneiss|23309|5|Briefly described|p47, 336, 375||Cambrian|Age: 514+/-5 Ma.||||||
15851|Rathjen Gneiss|23317|4|Described|p377, p379-388|Cambrian|Cambrian|Granitic intrusion in the Adelaide Fold Belt. Coarse medium-grained orthogneiss of granitic to granodioritic composition.  I-type.|514.6+/-5.9 Ma U/Pb SHRIMP magmatic cryst.|||||16-MAR-22
15851|Rathjen Gneiss|23818|6|Mentioned|p106|||||||||
15851|Rathjen Gneiss|23869|5|Briefly described|p15 Fig.  3|Cambrian|Cambrian|||||||
15851|Rathjen Gneiss|23996|5|Briefly described|p352|Cambrian|Cambrian|Age: 516+/-4Ma.||||||
15851|Rathjen Gneiss|24361|5|Briefly described|p50|Cambrian|Cambrian|Age: 514+/-4 Ma. Intrudes Carrickalinga Head Formation.||||||
15851|Rathjen Gneiss|24402|5|Briefly described|p324|||Palaeoproterozoic zircons present.  Geological Province: Delamerian Orogen||||||
15851|Rathjen Gneiss|24465|5|Briefly described|p345|Early Cambrian|Early Cambrian|Intrudes Kanmantoo Group.||||||
15851|Rathjen Gneiss|24593|6|Mentioned|p625 Fig. 9|Paleozoic|Paleozoic|||||||07-NOV-08
15851|Rathjen Gneiss|24599|5|Briefly described|p498|Early Cambrian|Early Cambrian|Age: 514 +/-5Ma.  Geological Province: Adelaide Fold Belt.||||||
15851|Rathjen Gneiss|32432|6|Mentioned|Fig.2|||See also Table 1||||||
15851|Rathjen Gneiss|32457|4|Described|p100|||||||||
15851|Rathjen Gneiss|34536|6|Mentioned|Map legend|Early Ordovician|Late Cambrian|U.Camb. - L.Ord.||||||
15851|Rathjen Gneiss|34612|6|Mentioned|p106|||||||||
15851|Rathjen Gneiss|35358|6|Mentioned|p8|||||||||
15851|Rathjen Gneiss|39880|6|Mentioned|p352|||||||||
15851|Rathjen Gneiss|40501|6|Mentioned|p118|||||||||
15851|Rathjen Gneiss|41947|6|Mentioned|Fig.2 P17|||||||||
15851|Rathjen Gneiss|42272|5|Briefly described|p410|||||||||
15851|Rathjen Gneiss|42275|5|Briefly described|p466|||||||||
15851|Rathjen Gneiss|42499|5|Briefly described|Map legend|Ordovician|Late Cambrian|||||||
15851|Rathjen Gneiss|42884|5|Briefly described|Fig.1 P11|||||||||
15851|Rathjen Gneiss|43190|6|Mentioned|Fig.1,p28.|||||||||
15851|Rathjen Gneiss|43703|6|Mentioned|p75|Middle Cambrian|Early Cambrian|Age: 516+/-4 Ma||||||
15851|Rathjen Gneiss|44133|5|Briefly described|p51 Fig. 7.18, 56 Table 7.3|Cambrian|Cambrian|Highly foliated granitic gneiss. I-Type. Age: 516 +/- 4Ma.||||||
15851|Rathjen Gneiss|45003|14|Not recorded|p328|||||||||
15851|Rathjen Gneiss|50154|5|Briefly described|p24|Early Cambrian|Early Cambrian|Age: 514 +/- 5 Ma (Foden et al., 1999)||||||
15851|Rathjen Gneiss|61046|5|Briefly described|p8 Fig. 2|||Granitic gneiss.||||||
15851|Rathjen Gneiss|61307|6|Mentioned|p12, p14 Fig. 6|Early Cambrian|Early Cambrian|Oldest felsic intrusive phase recognisable in Adelaide Fold Belt. Outcrops as a thin sheet-like body folded about upright fold structures in the eastern Mount Lofty Ranges. Age: 516+/-5Ma. Geol Prov: Adelaide F.B. See also p27.||||||
15851|Rathjen Gneiss|62742|5|Briefly described|p699 Fig. 2|Early Cambrian|Early Cambrian|||||||
15851|Rathjen Gneiss|62744|5|Briefly described|p709 Fig. 2|Early Cambrian|Early Cambrian|||||||
15851|Rathjen Gneiss|64647|6|Mentioned|p38, p41|||Intrudes the Kanmantoo Group.||||||
15851|Rathjen Gneiss|65686|5|Briefly described|p420|Cambrian|Cambrian||U-Pb: 514 +/- 4 Ma.|||Intrudes the Kanmantoo Group.|Granitoid.|07-MAY-12
15851|Rathjen Gneiss|67103|5|Briefly described|p613|||Zircons sourced from Kanmantoo Group.|514 +/- 5 Ma.||||Pre- or early syn-tectonic granite.|
15851|Rathjen Gneiss|67536|5|Briefly described|Map Legend|Tremodocian|Ediacaran|Kanmantoo Province; basement to Murray Basin.|ca. 564 +/- 57 Ma - 486 +/- 6 Ma||||Pre/syn-Delamerian felsic intrusive rocks.|
15851|Rathjen Gneiss|68314|5|Briefly described|p749, p754, p755 Fig.6, p757|Early Cambrian|Early Cambrian|Delamerian Orogen. Underwent high-grade metamorphism: high-U overgrowths on zircons are dated 503 +/- 7 Ma. Ages inferred from Fig.6.|514 +/- 5 Ma (Foden et al., 1999).|||||
15851|Rathjen Gneiss|68822|6|Mentioned|p331|Stage 4|Stage 3|S-type granite?|514 +/- 5 Ma, zircon age (Foden et al. 1999)|||||
15851|Rathjen Gneiss|70025|6|Mentioned|p28|||Syn-tectonic gneiss with U-Pb age 514+\-14 Ma (Foden et al., 1999) coeval with convergence and final docking of Tyennan and Pedder zones along Mt Hobhouse Fault.|514+\-4 Ma|||||
15851|Rathjen Gneiss|71139|6|Mentioned|p153, 155, 158|||Oldest deformed (Delamerian Orogeny) granite in the southern Adelaide fold belt. Pb, Th, U concentrations and Pb isotope data tabulated.|514 Ma (Foden et al., 1999).||||I-type.|
15851|Rathjen Gneiss|71322|5|Briefly described|p52 Fig.1, p73|Ordovician|Cambrian|Pre/syn Delamerian (564+/-57 Ma - 486 +/-6 Ma).|514 +/- 6.5 Ma (Foden et al., 1999).||||Felsic intrusive rocks.|
15851|Rathjen Gneiss|71593|5|Briefly described|p23|Cambrian|Cambrian|The oldest known pre to syn-tectonic granitic rock in the Fleurieu Peninsula.|514 +/- 5 Ma (Foden et al., 1999)|||||
15968|Redan Gneiss|6823|5|Briefly described|p205, 207-208|Palaeoproterozoic|Palaeoproterozoic|Features a metamorphic age of roughly <1590 Ma, , both of Love (1992).|1827 +/- 18 Ma (magmatic age, SHRIMP U-Pb)|||Underlies the Thackaringa Group.||26-MAR-22
15968|Redan Gneiss|22553|5|Briefly described|fig2p77|Orosirian|Orosirian|Part of Willyama Supergroup.||||||23-JUN-08
15968|Redan Gneiss|22575|6|Mentioned|p179 Fig.2|||in the Broken Hill Block||||||
15968|Redan Gneiss|22771|6|Mentioned|Table12.2p45|||||||||
15968|Redan Gneiss|22857|5|Briefly described|p45 Tb. 12.2, p392 App1 Tb.A1.1|Paleoproterozoic|Paleoproterozoic|Of the Willyama Supergroup. Max. thickness: 1.5km. Geological Province: Willyama Fold Belt.||||||07-NOV-08
15968|Redan Gneiss|22884|5|Briefly described|p41, p43 Fig. 3|||Geological province: Broken Hill Domain. Correlates with similar George Mine Formation.||||||26-MAR-09
15968|Redan Gneiss|22962|6|Mentioned|p74||Statherian|||||||
15968|Redan Gneiss|22965|6|Mentioned|Fig 1||Statherian|||||||
15968|Redan Gneiss|22966|5|Briefly described|p2,Fig 1||Proterozoic|Early rift stage of development.||||||
15968|Redan Gneiss|23248|5|Briefly described|Fig2p169|||||||||
15968|Redan Gneiss|24197|5|Briefly described|p29|Paleoproterozoic|Paleoproterozoic|Rocks are leucocratic, high in silica and are usually albitic. Age: ~1710Ma. Geological Province: Broken Hill Domain.||||||07-FEB-11
15968|Redan Gneiss|24307|5|Briefly described|p968 Fig. 3|Proterozoic|Proterozoic|||||||
15968|Redan Gneiss|29864|6|Mentioned|p263|||||||||
15968|Redan Gneiss|33287|6|Mentioned|Fig.1|||||||||
15968|Redan Gneiss|33875|6|Mentioned|p24|||Radioactivity.||||||
15968|Redan Gneiss|34071|6|Mentioned|Map legend|Mesoproterozoic|Paleoproterozoic|Lower to Middle Proterozoic||||||07-NOV-08
15968|Redan Gneiss|34468|6|Mentioned|Map legend|Mesoproterozoic|Paleoproterozoic|Willyama Complex. Middle - Lower Proterozoic||||||07-NOV-08
15968|Redan Gneiss|42530|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
15968|Redan Gneiss|42537|6|Mentioned|Fig.2 P5|||||||||
15968|Redan Gneiss|42595|6|Mentioned|Fig. 2 P5|||||||||
15968|Redan Gneiss|42897|2|Defined|p332|Proterozoic||see also Fig.3, p321.||||||29-MAY-07
15968|Redan Gneiss|43052|6|Mentioned|Fig.4.22|||||||||
15968|Redan Gneiss|43086|6|Mentioned|Fig.3|||||||||
15968|Redan Gneiss|43263|6|Mentioned|Map Legend||Paleoproterozoic|||||||07-NOV-08
15968|Redan Gneiss|43273|5|Briefly described|Map Legend||Paleoproterozoic|Of Willyama Supergroup.||||||07-NOV-08
15968|Redan Gneiss|43464|14|Not recorded|Map Legend|Mesoproterozoic|Paleoproterozoic|(Provisional Edition)||||||07-NOV-08
15968|Redan Gneiss|43572|6|Mentioned|p5||Paleoproterozoic|||||||07-NOV-08
15968|Redan Gneiss|46598|5|Briefly described|p302|||||||||
15968|Redan Gneiss|50045|5|Briefly described|p116 Fig. 3|||Geological Province: Broken Hill Block. Of the Willyama Supergroup. Overlain by Ednas Gneiss.||||||31-MAY-07
15968|Redan Gneiss|50606|5|Briefly described|p1.3, Table 1.1|Paleoproterozoic|Paleoproterozoic|Of the Redan Suite. Geological Province: Broken Hill Block. Age: 1570-1920Ma (U-Pb).||||||07-NOV-08
15968|Redan Gneiss|50619|5|Briefly described|p175|Paleoproterozoic|Paleoproterozoic|Of the Willyama Supergroup. Geological Province: Broken Hill Block.||||||07-NOV-08
15968|Redan Gneiss|60485|5|Briefly described|p28 Fig. 2|||Of the Thackaringa Group? Geological Province: Broken Hill Domain.||||||28-APR-05
15968|Redan Gneiss|61606|5|Briefly described|p4 Fig.2|||||||||
15968|Redan Gneiss|61735|5|Briefly described|p634, p635 Fig. 1|Paleoproterozoic|Paleoproterozoic|Part of the Redan Block.See also p636 Fig. 2.||||||04-JUN-15
15968|Redan Gneiss|62536|6|Mentioned|p635-636|||Redan Block, Broken Hill area.||||||
15968|Redan Gneiss|62592|5|Briefly described|p14, p16 Fig.2.2.|||Possibly a part-equivalent of Ethiudna Subgroup.||Basal unit in Thackaringa Group.||||
15968|Redan Gneiss|62993|6|Mentioned|p37|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain.|1710+/-4 Ma|||||19-DEC-21
15968|Redan Gneiss|63102|5|Briefly described|p13|Statherian|Statherian|Geological province: Broken Hill Domain, Curnamona Province.||Unit of Thackaringa Group.||||22-OCT-19
15968|Redan Gneiss|63489|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
15968|Redan Gneiss|63519|5|Briefly described|p10 Fig. 3|Paleoproterozoic|Paleoproterozoic|Age: 1682+/-3Ma. Geological Province: Redan Sub-block.||||||07-NOV-08
15968|Redan Gneiss|63866|5|Briefly described|p36, p40|||Redan Subdomain of the Broken Hill Domain, Curnamona Province.|c. 1710 Ma|Willyama Supergroup||Overlain by the Ednas Formation, Mulculca Formation and the Farmcote Gneiss.||
15968|Redan Gneiss|64097|5|Briefly described|p302, p309|Paleoproterozoic|Paleoproterozoic|Lower unit of Rantyga Gp in Redan geophysical zone in SE Broken Hill Domain. Underlies Farmcote Gneiss. Age:~1710+/-4Ma to 1704+/-13Ma (age evidence analysed). Laminated albite-qtz-hornblende-magnetite rock, and albite-qtz-magnetite rock.||||||07-FEB-11
15968|Redan Gneiss|64316|5|Briefly described|p532, p533 Fig. 1|||In lower Willyama Supergroup. Part of the amphibole-quartz-albite-magnetite Redan geophysical Zone forming a magnetic high regionally. Geological Province: Broken Hill Block. Also referred to as Redan Gneisses.||||||07-FEB-11
15968|Redan Gneiss|64741|5|Briefly described|p301 Fig. 4|Paleoproterozoic|Paleoproterozoic|Of the Rantyga Group. Age: 1710+/-4Ma. Geological province: Broken Hill Domain.||||||07-FEB-11
15968|Redan Gneiss|64744|6|Mentioned|p353 Fig.4. |Statherian|Statherian|Broken Hill Domain.||Unit in Willyama Supergroup.||Is overlain by Clevedale Migmatite.||
15968|Redan Gneiss|64944|5|Briefly described|p27, p28 Fig. 1|Paleoproterozoic|Paleoproterozoic|Age: 1710+/-4Ma. Geological province: Broken Hill Domain. Similar in age to the intrusive part (the Amaroo Subsuite) of Basso Suite in Olary Domain.||||||07-FEB-11
15968|Redan Gneiss|66302|5|Briefly described|p8, p36 Fig.9, p39, p76 Fig.20|Statherian|Statherian|Redan Domain, Curnamona Province.|1710 +/- 4 Ma (Stevens et al, 2008)|Rantyga Group||Overlain by the Ednas Gneiss.||
15968|Redan Gneiss|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Broken Hill Domain.|1710 +/- 4 Ma.|Rantyga Group.||||
15968|Redan Gneiss|67581|6|Mentioned|p45|||||Willyama Supergroup.||||
15968|Redan Gneiss|68126|6|Mentioned|p26, p30|||Oldest rocks in the Broken Hill Domain, Curnamona Province.|1710+/-4 Ma; 1704+/-13 Ma (Stevens et al., 2008).|||||
15968|Redan Gneiss|70000|5|Briefly described|p34-35|Statherian|Statherian|The basal gneiss may represent an altered metavolcanic rock.|1710 +/- 4 Ma (Stevens, Page and Crooks 2008).|Unit in Rantyga Group.||Correlated with uppermost Curnamona Group.|Includes basal quartz-albite-K-feldspar-magnetite gneiss.|
15968|Redan Gneiss|70014|5|Briefly described|Map legend|||||Unit in Willyama Supergroup.||Is overlain by Ednas Gneiss.|Albite-hornblende-quartz rock, sodic plagioclase-quartz-magnetite rock, minor quartz-albite-magnetite gneiss.|
15968|Redan Gneiss|70015|5|Briefly described|Map legend|Statherian|Statherian|Mineral deposits (if any) are shown.||Unit in Rantyga Group.|||Albite-quartz-hornblende-magnetite (+/- K feldspar +/- clinopyroxene) gneiss, with hornblende-rich laminations and thicker (up to 20mm) layers of quartz-feldspar.|
15968|Redan Gneiss|70405|6|Mentioned|p9 table 1, p40|Paleoproterozoic|Paleoproterozoic||1710 Ma||||Metavolcanic gneiss and calc-albitic metasediments; highly magnetic.|
15968|Redan Gneiss|70657|5|Briefly described|p10 Fig.4, p13 Fig.6, p15|Statherian|Statherian|Curnamona Province; Broken Hill Domain. Shown as Ethiudna Subgroup + Redan Gneiss in Fig.4.but separately in Fig. 6. Relationship with Ethiudna Subgroup is unclear. In Willyama Supergroup. Age also shown as ~1710 Ma in Fig.6 and as 1710 +/- 4 Ma on p15.|~1720-1715 Ma|Rantyga Group||Underlies Thackaringa Group and Ednas Gneiss.||
15968|Redan Gneiss|70658|6|Mentioned|p15-16|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain, Curnamona Province.|1710 +/- 4 Ma.|||||
15968|Redan Gneiss|72461|5|Briefly described|p16 fig 9|||Redan sub-block of the Broken Hill Block.|1710 +/- 4 Ma|Rantyga Group||Overlain by the Ednas Gneiss.||
15968|Redan Gneiss|73243|6|Mentioned|p53 Fig.2|||||||||
15968|Redan Gneiss|73482|5|Briefly described|p422 Fig.3|Statherian|Statherian|Redan sub-block.|1710+/-4 Ma|Rantyga Group||||
15968|Redan Gneiss|73575|5|Briefly described|p828 Fig.2, p829 Fig.3|Statherian|Statherian|Redan Geophysical Zone.|1710+/-4 Ma|Rantyga Group||||
15996|Reedy Creek Granodiorite|22726|6|Mentioned|p233|||||||||
15996|Reedy Creek Granodiorite|42275|6|Mentioned|Table 3 P475|||Variation on Victoria's Reedy Creek Quartz Diorite?||||||
15996|Reedy Creek Granodiorite|43190|6|Mentioned|Fig.1,p28.|||||||||
15996|Reedy Creek Granodiorite|50437|5|Briefly described|p1.7, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Kimberley Region. Of the Dougalls Suite. Used interchangeably with Reedy Creek Tonalite.||||||07-NOV-08
15996|Reedy Creek Granodiorite|61307|5|Briefly described|p12, p14 Fig. 6||Late Cambrian|Geochemically forms part of the older I-type suite, the Reedy Creek Diorite. Age: ~490Ma.  See also p26.||||||
15996|Reedy Creek Granodiorite|68314|5|Briefly described|p754, p755 Fig.6, p756|Late Cambrian|Late Cambrian|Delamerian Orogen. Magmatism coincides with post-collision magmatic event in Tasmania (ignimbrites) and W Victoria. Ages inferred from Fig.6.|496 +/- 1 and 494 +/- 1 Ma (Foden et al. 2004).|||||
16036|Renmark Group|2967|5|Briefly described|p14-15, 17-24, 27-31, 34-35, 39, 46-47|Miocene|Palaeocene|Lawrence (1975); previously the Renmark Beds of Harris (1971); see references p14, 33. Murray Basin. Locally the Calivil Formation sediments fill in valleys incised into this Group. Deep aquifers. See also p79, 96, 105, 110, 112, 128, 151, 155, 178, 336.|||Olney Formation, Warina Sand.|Is overlain by Ettrick Marl and Geera Clay (Murray Group). Elsewhere, is separated from the overlying Parilla Sand and Calivil Formation by the Mologa Surface.|A widespread, thick suite of fine-grained sands and carbonaceous sediments.|
16036|Renmark Group|10010|5|Briefly described|p12 Fig. 3|Miocene|Paleocene|Overlain by Olney Formation. Geological Province: Murray Basin.||||||13-AUG-07
16036|Renmark Group|22487|6|Mentioned|p212 Fig. 13|Tertiary|Tertiary|Geological province: eastern Murray Basin.||||||11-SEP-08
16036|Renmark Group|22531|6|Mentioned|p6|Eocene|Eocene|||||||
16036|Renmark Group|22587|6|Mentioned|p79 Fig.7|Late Eocene|Late Paleocene|||||||
16036|Renmark Group|22712|5|Briefly described|p132|||||||||
16036|Renmark Group|22756|6|Mentioned|P28|||||||||
16036|Renmark Group|22773|6|Mentioned|p351|||||||||
16036|Renmark Group|22782|6|Mentioned|p15|||||||||
16036|Renmark Group|22799|2|Defined|p25|Middle Miocene|Paleocene|||||||
16036|Renmark Group|22857|5|Briefly described|p351, p352 Fig.24.8|Miocene|Paleocene|Age: ~60Ma. Geological Province: Murray Basin. See also p353 Fig. 24.9.||||||
16036|Renmark Group|22887|6|Mentioned|p32, p75|Oligocene|Eocene|Fluvial||||||
16036|Renmark Group|22893|5|Briefly described|p25 fig9|Tertiary|Tertiary|||||||
16036|Renmark Group|22971|4|Described|p 26||Tertiary|||||||
16036|Renmark Group|23179|6|Mentioned|Fig.2||Early Oligocene|Murray Basin.||||||
16036|Renmark Group|23226|6|Mentioned|p889||Oligocene|||||||
16036|Renmark Group|23230|4|Described|Table4-1p40, 41, 43-4|Oligocene|Paleocene|||||||
16036|Renmark Group|23234|6|Mentioned|p88|Oligocene|Paleocene|||||||
16036|Renmark Group|23252|5|Briefly described|Map Legend||Tertiary|||||||
16036|Renmark Group|23402|5|Briefly described|p31|Early Miocene|Paleocene|Geological Province: Murray Basin||||||
16036|Renmark Group|23884|5|Briefly described|p153, p155 Fig. 13.2|Middle Miocene|Late Paleocene|Geological Province: Murray Basin.||||||
16036|Renmark Group|23921|5|Briefly described|p1109|Middle Miocene|Eocene|Geological Province: Murray Basin.||||||
16036|Renmark Group|24105|5|Briefly described|p159|||Overlain by Wunghnu Group.||||||13-MAR-07
16036|Renmark Group|24106|5|Briefly described|p184|Miocene|Miocene|Geological Province: Murray Basin.||||||
16036|Renmark Group|24177|4|Described|p69|Early Miocene|Paleocene|Overlain by the Calivil Formation. Age: ~65 Ma. Comprised of Warina Sand and Olney Formation. Correlated with Pebble Point, Wiridgil and Eastern View formations of the Wangerrip Group in Otway Basin. Geological Province: Murray Basin.||||||06-FEB-15
16036|Renmark Group|24239|5|Briefly described|p11|Tertiary|Tertiary|Geological Province: Murray Basin.||||||
16036|Renmark Group|24328|5|Briefly described|Map legend|Paleogene|Paleogene|||||||07-NOV-08
16036|Renmark Group|24329|5|Briefly described|Map legend|Paleogene|Paleogene|||||||07-NOV-08
16036|Renmark Group|24383|6|Mentioned|p58|||||||||
16036|Renmark Group|24439|6|Mentioned|p37|||Time equivalent of parts of lower Loddon River Group.  Geological Province: Murray Basin.||||||
16036|Renmark Group|24470|6|Mentioned|p473|||||||||
16036|Renmark Group|24551|5|Briefly described|p320, 417, 421, 543|Ealry Oligocene|Paleocene|Maximum Thickness: 300m.||||||
16036|Renmark Group|24563|5|Briefly described|p485, p486|||Geological Province: Murray Basin.||||||
16036|Renmark Group|24574|6|Mentioned|p705|||Geological Province: Murray Basin||||||
16036|Renmark Group|29355|6|Mentioned|p179|||||||||
16036|Renmark Group|29591|6|Mentioned|Table 20|||||||||
16036|Renmark Group|30581|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
16036|Renmark Group|30934|6|Mentioned|Map legend|Eocene|Eocene|Equivalence with Wangerrip Group||||||
16036|Renmark Group|30935|6|Mentioned|Map legend|Tertiary|Tertiary|Subsurface||||||
16036|Renmark Group|30936|6|Mentioned|Map legend|Eocene|Eocene|||||||
16036|Renmark Group|31625|6|Mentioned|Fig. 5.2|||Palaeocene-Eocene||||||
16036|Renmark Group|31654|6|Mentioned|Map legend|Eocene|Eocene|||||||
16036|Renmark Group|31713|6|Mentioned|p16|||||||||
16036|Renmark Group|31741|6|Mentioned|p6|||||||||
16036|Renmark Group|31745|6|Mentioned|Map legend|Eocene|Eocene|||||||
16036|Renmark Group|31746|3|Fully described|p191|||||||||
16036|Renmark Group|31747|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
16036|Renmark Group|31922|6|Mentioned|Fig.2|||||||||
16036|Renmark Group|31951|6|Mentioned|p7|||||||||
16036|Renmark Group|31952|6|Mentioned|p7|||||||||
16036|Renmark Group|31953|6|Mentioned|p9|||||||||
16036|Renmark Group|32225|6|Mentioned|p22|||||||||
16036|Renmark Group|32315|6|Mentioned|p4|||||||||
16036|Renmark Group|32862|6|Mentioned|Fig. 3|||Section from boreholes||||||
16036|Renmark Group|34312|5|Briefly described|p46|||L.Tertiary||||||
16036|Renmark Group|34313|6|Mentioned|p165|||||||||
16036|Renmark Group|34735|4|Described|p31|||||||||
16036|Renmark Group|34757|6|Mentioned|p45|||||||||
16036|Renmark Group|35091|4|Described|p7|||||||||
16036|Renmark Group|35094|6|Mentioned|p9|||||||||
16036|Renmark Group|35172|6|Mentioned|p127|||||||||
16036|Renmark Group|35285|5|Briefly described|p413|||||||||
16036|Renmark Group|35498|6|Mentioned|Fig.1|||||||||
16036|Renmark Group|36305|6|Mentioned|p358|||||||||
16036|Renmark Group|37873|6|Mentioned|p1|||||||||
16036|Renmark Group|38293|4|Described|Table 1|||||||||
16036|Renmark Group|38601|5|Briefly described|p7|||||||||
16036|Renmark Group|39329|6|Mentioned|p483|||||||||
16036|Renmark Group|39929|6|Mentioned|p269|||||||||
16036|Renmark Group|40599|5|Briefly described|p19|||||||||
16036|Renmark Group|40795|5|Briefly described|p80|||Mention p82.||||||13-MAR-07
16036|Renmark Group|41068|5|Briefly described|p65|||.||||||13-MAR-07
16036|Renmark Group|41423|6|Mentioned|p284|||||||||
16036|Renmark Group|41517|6|Mentioned|p139|||||||||
16036|Renmark Group|41765|4|Described|p34|||||||||
16036|Renmark Group|41868|5|Briefly described|p550|||||||||
16036|Renmark Group|42125|5|Briefly described|p132|||||||||
16036|Renmark Group|42126|6|Mentioned|p149, p152|||||||||
16036|Renmark Group|42127|5|Briefly described|p218|||See also Fig.1||||||
16036|Renmark Group|42129|6|Mentioned|p254|||See also Fig.6||||||
16036|Renmark Group|42130|6|Mentioned|p264|||||||||
16036|Renmark Group|42133|6|Mentioned|p301|||||||||
16036|Renmark Group|42134|4|Described|p340|||||||||
16036|Renmark Group|42137|5|Briefly described|p367|||||||||
16036|Renmark Group|42138|6|Mentioned|p388|||||||||
16036|Renmark Group|42184|6|Mentioned|p351|||||||||
16036|Renmark Group|42454|4|Described|p11|early Miocene|middle Eocene|||||||
16036|Renmark Group|42455|5|Briefly described|Map legend|early Miocene|middle Eocene|||||||
16036|Renmark Group|42623|5|Briefly described|p2|||aquifer||||||
16036|Renmark Group|42648|6|Mentioned|p45|||||||||
16036|Renmark Group|42827|3|Fully described|p265|||see also Fig 8.4||||||
16036|Renmark Group|42881|4|Described|Fig.3, p84|||||||||01-NOV-22
16036|Renmark Group|42966|2|Defined|p91|Middle Miocene|Paleocene|||||||
16036|Renmark Group|43195|5|Briefly described|Map Legend|Early Oligocene|Middle Eocene|See also commentary on back of map.||||||
16036|Renmark Group|43218|4|Described|Fig.3,p22||Tertiary|||||||
16036|Renmark Group|43493|6|Mentioned|32|||||||||
16036|Renmark Group|43655|5|Briefly described|p40-846|||||||||
16036|Renmark Group|43669|6|Mentioned|p9|||||||||
16036|Renmark Group|43780|5|Briefly described|p6|||||||||
16036|Renmark Group|43791|6|Mentioned|p371|||||||||
16036|Renmark Group|43804|6|Mentioned|p47|||||||||
16036|Renmark Group|44093|6|Mentioned|p145 App. 1|||||||||
16036|Renmark Group|44133|5|Briefly described|p158|Early Oligocene|Late Paleocene|Geological Province: Murray Basin. Includes: Warina Sand, Olney Formation.||||||
16036|Renmark Group|44188|6|Mentioned|Map Legend|Miocene|Eocene|Includes the Olney Formation. Geological province: Murray Basin.||||||15-MAY-08
16036|Renmark Group|44191|5|Briefly described|Map Legend||Middle Miocene|||||||
16036|Renmark Group|45168|6|Mentioned|p6|||See also Table 1.||||||
16036|Renmark Group|49038|5|Briefly described|p24|||See also p40||||||13-MAR-07
16036|Renmark Group|49040|6|Mentioned|p10|||||||||
16036|Renmark Group|50154|2|Defined|p26, p132-135|Middle Miocene|Late Paleocene|Geological Province: Murray Basin. Max. thickness: over 300m. Overlain by the Murray Group, Calivil Formation and Parilla Sand. Overlies the Grampians Group and Rocklands Volcanic Group. Correlates with the Wangerrip & Nirranda groups.||||||15-SEP-04
16036|Renmark Group|50155|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|Fluvio-lacustrine; gravel, quartz sand, silt and clay||||||
16036|Renmark Group|50156|5|Briefly described|Map Legend|Miocene|Paleocene|Fluvio-lacustrine deposits: gravel, quartz sand, silt and clay; pyritic, ferruginised, unconsolidated to poorly unconsolidated.||||||
16036|Renmark Group|50157|5|Briefly described|Map Legend|Miocene|Paleocene|Overlies Eumeralla Formation. Overlain by Ettrick Marl. Fluvio-lacustrine deposits: gravel, quartz sand, silt and clay; pyritic, ferruginised, unconsolidated to poorly unconsolidated.||||||13-MAR-07
16036|Renmark Group|50158|5|Briefly described|Map Legend|Miocene|Paleocene|Fluvio-lacustrine deposits: gravel, quartz sand, silt and clay; pyritic, ferruginised, unconsolidated to poorly consolidated.||||||24-AUG-04
16036|Renmark Group|50159|5|Briefly described|Map Legend|Miocene|Paleocene|Fluvio-lacustrine deposits: gravel, quartz sand, silt and clay; pyritic, ferruginised, unconsolidated to poorly unconsolidated.||||||
16036|Renmark Group|50160|5|Briefly described|Map Legend|Miocene|Paleocene|||||||
16036|Renmark Group|50161|5|Briefly described|Map Legend|Miocene|Paleocene|Fluvio-lacustrine deposits: gravel, quartz sand, silt and clay; pyritic, ferruginised, unconsolidated to poorly unconsolidated.||||||
16036|Renmark Group|50162|5|Briefly described|Map Legend|Miocene|Paleocene|Fluvio-lacustrine deposits: gravel, quartz sand, silt and clay; pyritic, ferruginised, unconsolidated to poorly unconsolidated.||||||
16036|Renmark Group|50163|5|Briefly described|Map Legend|Miocene|Paleogene|Fluvio-lacustrine deposits: gravel, quartz sand, silt and clay; pyritic, ferruginised, unconsolidated to poorly unconsolidated.||||||07-NOV-08
16036|Renmark Group|50164|5|Briefly described|Map Legend|Miocene|Paleocene|Overlies Otway Group. Fluvio-lacustrine deposits: gravel, quartz sand, silt and clay; pyritic, ferruginised, unconsolidated to poorly unconsolidated.||||||25-JUN-04
16036|Renmark Group|60421|5|Briefly described|p409, 415|Oligocene|Paleocene|||||||07-NOV-08
16036|Renmark Group|60451|5|Briefly described|p95 Fig. 61|||||||||
16036|Renmark Group|60452|5|Briefly described|p14, 15|Cenozoic|Cenozoic|Includes Warina Sand at base. See also p68.||||||19-NOV-08
16036|Renmark Group|60461|5|Briefly described|Map legend|Eocene|Paleocene|Includes the Olney Formation.||||||06-OCT-04
16036|Renmark Group|60491|4|Described|p21|Oligocene|Late Eocene|Includes the Olney Formation and Warina Sand. Disconformably overlain by the Parilla Sand. Max. thickness: 100m. Palynological studies yield late Eocene to Oligocene ages.||||||
16036|Renmark Group|60492|5|Briefly described|Map Legend|Oligocene|Paleocene|Overlies the Glenloth Suite and Pyrenees Formation. Overlain by Parilla Sand. Fluviolacustrine to marginal marine: carbonaceous silt and fine sand with calcareous bands and marine fossils; some lignite rich bands.||||||30-SEP-04
16036|Renmark Group|60538|6|Mentioned|p473 Fig.12|||||||||
16036|Renmark Group|60591|5|Briefly described|Map Legend|Paleocene|Paleocene|Unconformably overlies the Urana Formation. Overlain by the Calivil Formation. Fluvio-lacustrine deposits: gravel, quartz sand, silt and clay; pyritic, ferruginised, unconsolidated to poorly unconsolidated.||||||
16036|Renmark Group|60592|5|Briefly described|Map Legend|Paleocene|Paleocene|Unconformably overlies the Urana Formation. Overlain by the Calivil Formation. Fluvio-lacustrine deposits: gravel, quartz sand, silt and clay; pyritic, ferruginised, unconsolidated to poorly unconsolidated.||||||
16036|Renmark Group|60593|5|Briefly described|Map Legend|Paleocene|Paleocene|Unconformably overlies the Urana Formation. Overlain by the Calivil Formation. Fluvio-lacustrine deposits: gravel, quartz sand, silt and clay; pyritic, ferruginised, unconsolidated to poorly unconsolidated.||||||
16036|Renmark Group|60595|5|Briefly described|Map Legend|Paleocene|Paleocene|Unconformably overlies the Urana Formation. Overlain by the Calivil Formation. Fluvio-lacustrine deposits: gravel, quartz sand, silt and clay; pyritic, ferruginised, unconsolidated to poorly unconsolidated.||||||
16036|Renmark Group|60596|5|Briefly described|Map Legend|Paleocene|Paleocene|Unconformably overlies the Urana Formation. Overlain by the Calivil Formation. Fluvio-lacustrine deposits: gravel, quartz sand, silt and clay; pyritic, ferruginised, unconsolidated to poorly unconsolidated.||||||
16036|Renmark Group|60597|5|Briefly described|Map Legend|Eocene|Paleocene|Fluvio-lacustrine deposits: no distinctive magnetic responses.||||||
16036|Renmark Group|60599|2|Defined|p15, p84-85|Early Miocene|Middle Eocene|Formerly part of Knight Group (Sprigg and Boutakoff 1953). Originally informally divided into 'lower' and 'upper' Renmark Beds. Lithological details included. Overlain by Murray Gp+ Calivil Fm.||||||27-OCT-08
16036|Renmark Group|61155|5|Briefly described|p3, p18|Middle Miocene|Late Paleocene|Comprises Warina Sand, Olney Formation Buccleuch beds. Includes fluvial-lacustrine unconsolidated carbonaceous clastics. Age: ~53-~14.5Ma. Extends into the Miocene in eastern Murray Basin (Olney Formation). Geological Province: Murray Basin.||||||
16036|Renmark Group|61180|6|Mentioned|p37|||Contains brown coal seams up to 40m thick in some places.||||||
16036|Renmark Group|61181|5|Briefly described|p153 Fig. 47|||Sandy carbonaceous clay over sand and minor clay.||||||
16036|Renmark Group|61183|6|Mentioned|p133|||Geological Province: Murray and Otway Basins.||||||
16036|Renmark Group|61185|5|Briefly described|p57, p58||Middle Paleocene|Includes Olney Formation and Warina Sand. Disconformably underlies Calivil Formation. Geological Province: Murray Basin.||||||07-FEB-11
16036|Renmark Group|61822|6|Mentioned|p107|Paleogene|Paleogene|||||||07-NOV-08
16036|Renmark Group|61825|6|Mentioned|p138|Cenozoic|Cenozoic|In Broken Hill region.||||||19-NOV-08
16036|Renmark Group|61841|5|Briefly described|p242|Early Oligocene|Paleocene|Gravels and clays. Geological Province: Murray Basin.||||||
16036|Renmark Group|61964|5|Briefly described|p17, p139|Miocene|Oligocene|Includes the Olney Formation. Geological Province: Murray Basin. Informally subdivided into lower, middle and upper parts.||||||
16036|Renmark Group|63066|5|Briefly described|p485|Tertiary|Tertiary|Geological Province: Murray Basin.||||||08-FEB-07
16036|Renmark Group|63460|5|Briefly described|p839 Fig. 2b|early Oligocene|Early Oligocene|Geological province: Murray Basin.||||||
16036|Renmark Group|63777|5|Briefly described|p1104 Fig. 1, p1105|Late Miocene|Paleocene|Overlain by Calival Formation. Geological Province: Murray Basin. Fluvial clays, sand silt and gravels.||||||
16036|Renmark Group|63887|5|Briefly described|p20, p21 Fig. 1|Early Oligocene|Paleocene|Includes; Warina Sand, Olney Fm and Buccleuch Fm. Floodplain and swamp environments dominates, resulting in deposition of carbonaceous sand, clay and silt. Minor marine incursion during Late Eocene marked by clay and marl.||||||
16036|Renmark Group|64237|5|Briefly described|p17, p18 Fig. 2|Middle Miocene|Late Oligocene|Underlies Murray Group.||||||
16036|Renmark Group|64612|5|Briefly described|p28|Cainozoic|Cainozoic|Down hill extension of White Hills Gravel. Unclear if White Hills Gravel intended to be included in Renamrk Group. Geological Province: Murray Basin.||||||06-FEB-15
16036|Renmark Group|64823|5|Briefly described|p1011|Cenozoic|Cenozoic|Overlain by Calivil Formation. Fluvial clays, silts, sands and gravels; paleochannel deposits. Geological province: Murray Basin.||||||
16036|Renmark Group|65552|5|Briefly described|p5 Fig. 3, p6, p11 Fig.6, p12, p13-14|Middle Miocene|Late Palaeocene|See also p23,25,26 App. 2,4,5. Contains Olney Formation and Warina Sand. Unconformably overlies basement, unconformably underlies Wunghnu Group and Loxton-Parilla Sands. Associated with moderate concentrations of heavy minerals.||||||
16036|Renmark Group|65969|5|Briefly described|p27 Tb.3.3, p30|Oligocene|Eocene|Overlain by Murray Group. Includes Olney Formation and White Hills Gravel.||||||
16036|Renmark Group|66002|5|Briefly described|p10 Tb.7, p12|Paleogene|Paleogene|Replaces Knight Group of Boutakoff and Sprigg (1953). Name based on Renmark Beds of Harris (1966). Correlated in part with (obsolete) Loddon River Group. Defined by Lawrence and Abele, 1976.||||||
16036|Renmark Group|66012|5|Briefly described|p17|Miocene|Paleocene|In Murray Basin. Includes Olney Formation. Paleocene to early Miocene|| ||||13-JUN-13
16036|Renmark Group|66286|5|Briefly described|p179.|Oligocene|Paleocene|Southern Murray Basin.|||Includes Warina Sand and Olney Formation.|||
16036|Renmark Group|67127|6|Mentioned|p73|||||||Overlies the Grampians Grou;p. Underlies the Geera Clay.||
16036|Renmark Group|67179|5|Briefly described|p579, p584|Miocene|Paleocene|Fluvio-lacustrine, overlying the Neoproterozoic and early Paleozoic sediments, metasediments and granitoids of the Murray Basin basement.||||Underlies the Loxton Sand, Duddo Limestone, Geera Clay and Bookpurnong Beds.||28-MAY-13
16036|Renmark Group|67462|5|Briefly described|Map legend.|Late Eocene||Murray Basin.|||Includes Warina Sand.|||
16036|Renmark Group|68116|5|Briefly described|Appendix, Map 29.|Miocene|Thanetian||||||Gravel, quartz sand, silt and clay: pyritic, ferruginised, unconsolidated to poorly consolidated.|
16036|Renmark Group|68140|6|Mentioned|p1699, p1700 Fig.1, p1704 Fig.5|Miocene|Paleocene|This name seems to be used interchangeably with Renmark Formation (see references p1698, p1699, p1701-1708).|||||Lower: fluvial silts, sands, gravels, and clay.|09-FEB-18
16036|Renmark Group|68189|6|Mentioned|p26, p29||||||Includes the Warina Sand (base) and the Olney Formation.|||
16036|Renmark Group|68194|5|Briefly described|p22|Oligocene|Eocene|Murray Basin. Lawrence (1975); Lawrence and Abele (1988). Thickness <50m.|||Includes Warina Sand, Olney Formation.|Is overlain by Murray Group.||
16036|Renmark Group|68715|5|Briefly described|p31 Fig.5|Eocene|Eocene|Murray Basin.|||Includes Warina Sand, Olney Formation.|||07-APR-17
16036|Renmark Group|69562|5|Briefly described|p674|||||||||09-FEB-18
16036|Renmark Group|69798|5|Briefly described|p4 Fig.2|Miocene|Eocene|Murray Basin.|||Olney Formation.|||06-FEB-18
16036|Renmark Group|70718|5|Briefly described|p17, p24, p103, 129|Middle Miocene|Middle Paleocene|Murray Basin. Is one of the primary aquifers in the Hay map sheet area. Deposited in a warm, moist climate with rates of swamp and flood plain alluvium being generally slow.|||Includes the Warina Sand, Olney Formation.||Lower sequences are dominated by light-brown or grey quartz sand whilst the upper sequences are increasingly dominated by argillaceous and carbonaceous sediments.|02-JUN-19
16036|Renmark Group|71593|5|Briefly described|p51-p52, p54|||Murray Basin.|||Includes the Olney Group and the Warina Sand.|Overlain by the Murray Group.||
16036|Renmark Group|72445|5|Briefly described|App.1, App.2 p1; App.6 p2 Fig.1; App.7|Miocene|Paleocene|Shown in App 7 Fig 4 (from Brown & Stephenson 1991). An extensive group ranging from the Paleocene conglomerates of the Warina Sand to the Miocene Mologa Surface in the eastern Murray Basin. App.2 is a .csv format file.  Identified in Stavely 04, 05, 06,07,09,10,11,12,14, 16.|||Includes Olney Formation, Warina Sand.|Overlies Nargoon Group, sharply; Moornambool Metamorphic Complex, Williamsons Road Serpentinite. Underlies Bookpurnong Fm, gradational; Wunghnu, Murray Grps, gradational/sharp; Winnambool Fm, sharply|Organic-rich muddy sand and sand. Sparse <1 m intervals of lignite.|
16036|Renmark Group|73118|6|Mentioned|p83|Miocene|Paleocene||||Olney Formation, Warina Sand.|||
16036|Renmark Group|73188|6|Mentioned|p320|Late Eocene|Late Eocene|Murray Basin.||||||
16036|Renmark Group|73228|4|Described|p50, p52-57, p60, p62|Early Oligocene|Late Paleocene|Murray Basin. [upper and lower informal subdivisions are occasionally used and once capitalised; interpreted as general terms rather than specific distinctions]. Dominated by marginal marine, fluvial to lacustrine sediments also with shallow marine and swamp depositional environments. Identified in Cooltong 1, Berri North 1, Nadda 1, Loxton 1, and Overland Corner 1 drillholes. Maximum thickness  330 m. Misspelt as Remark Group p51.|||Olney Formation, Buccleuch Formation, Warina Sand|Underlain by Coombool Member (Monash Formation). Overlain by Ettrick Formation and Murray Group.|Includes fine to coarse grained quartzose sand interbedded with clay and lime clay; pyritic, calcareous, fossiliferous, and glauconitic, with minor coal and lignite.|
16036|Renmark Group|73229|5|Briefly described|p66-67, p70-72, p74-75|Early Oligocene|Late Paleocene|Murray Basin. [Analysed using pXRF; see article]. Fluvial, lacustrine and swamp environments. Show in Fig. 1 as extending into the Miocene.|||Buccleuch Formation, Olney Formation, Warina Sand||Includes sandstone, carbonaceous sand; silt; clay; lignite.|01-NOV-22
16036|Renmark Group|73253|6|Mentioned|p15|||Murray Basin.||||||
16036|Renmark Group|73496|6|Mentioned|Map legend|Oligocene|Eocene|||||||
16036|Renmark Group|73505|5|Briefly described|p2, p10, p13, p36|Oligocene|Eocene|Murray Basin.|||Olney Formation, Warina Formation||Carbonaceous fluvial to paralic silt, clay; minor lignite.|
16059|Reynella Siltstone Member|22510|5|Briefly described|p40,table1|Adelaidean|Adelaidean|Age: Marinoan. At top of Elatina Formation in central Flinders Ranges. May be at top of Whyalla Sandstone on Stuart Shelf.||||||13-OCT-04
16059|Reynella Siltstone Member|23719|4|Described|p26|Neoproterozoic|Adelaidean|Of Elatina Formation. Overlying unit Wilpena Group. Underlying unit Willochra Subgroup. Geological Province: Gawler Craton. Max. thickness >35 m.||||||
16059|Reynella Siltstone Member|23818|5|Briefly described|p64 Fig.22, p71|Neoproterozoic|Neoproterozoic|Of the Willochra Sub-Group. Max. thickness: ~400 ft.||||||18-APR-05
16059|Reynella Siltstone Member|24195|5|Briefly described|p43 Fig.2|||Parent: Elatina Formation||||||
16059|Reynella Siltstone Member|24321|5|Briefly described|Map legend|Adelaidean|Adelaidean|Parent: Elatina Formation||||||
16059|Reynella Siltstone Member|29780|6|Mentioned|p41|||||||||
16059|Reynella Siltstone Member|30801|6|Mentioned|p5|||Wilmington Formation. Table P5-6.||||||
16059|Reynella Siltstone Member|30807|6|Mentioned|p103|||Suggested map symbol||||||
16059|Reynella Siltstone Member|33423|4|Described|p13|||||||||
16059|Reynella Siltstone Member|34535|6|Mentioned|Fig.22|||Wilmington Fm.||||||
16059|Reynella Siltstone Member|34536|6|Mentioned|Map legend|Adelaidean|Adelaidean|Marinoan||||||
16059|Reynella Siltstone Member|35255|6|Mentioned|Fig.7|||||||||
16059|Reynella Siltstone Member|35317|6|Mentioned|p399|||||||||
16059|Reynella Siltstone Member|35586|6|Mentioned|Fig.3|||||||||
16059|Reynella Siltstone Member|36898|6|Mentioned|p196|||||||||
16059|Reynella Siltstone Member|37461|5|Briefly described|p342|||See also Table 5.I||||||
16059|Reynella Siltstone Member|38157|6|Mentioned|Table IV|||||||||
16059|Reynella Siltstone Member|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Marinoan||||||
16059|Reynella Siltstone Member|39351|6|Mentioned|Map legend|Adelaidean|Adelaidean|Marinoan||||||
16059|Reynella Siltstone Member|40442|6|Mentioned|p10|||||||||
16059|Reynella Siltstone Member|40852|6|Mentioned|Fig.3.2|||||||||
16059|Reynella Siltstone Member|40914|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
16059|Reynella Siltstone Member|41005|6|Mentioned|Fig.2|||||||||
16059|Reynella Siltstone Member|41405|3|Fully described|p190|||||||||
16059|Reynella Siltstone Member|42090|5|Briefly described|p25|||||||||
16059|Reynella Siltstone Member|42222|6|Mentioned|Table 1 P4|||||||||
16059|Reynella Siltstone Member|42235|4|Described|p140|||See also Fig.3||||||
16059|Reynella Siltstone Member|42542|6|Mentioned|p8|||||||||
16059|Reynella Siltstone Member|42600|5|Briefly described|p7|||of Elatina Formation.||||||
16059|Reynella Siltstone Member|42882|6|Mentioned|p11|||of Elatina Formation||||||
16059|Reynella Siltstone Member|43052|5|Briefly described|p190,Table 6.1|||of Elatina Formation||||||
16059|Reynella Siltstone Member|67030|6|Mentioned|p409 Fig. 2|Cryogenian|Cryogenian|||Of Elatina Formation, Willochra Subgroup.||||26-APR-12
16059|Reynella Siltstone Member|70082|4|Described|p1-13,15-16|Cryogenian|Cryogenian|Flinders Ranges and Kulpara-Adelaide region. Also referred to interchangeably in text as Reynella Siltstone. Type section: (possibly? Not explicitly mentioned on p2) Wokurna DDH 6 drill core (S33.7134463, E138.1411738). Contains red beds and periglacial paleosols, correlable to those in Whyalla Sandstone and Cattle Grid Breccia. Sedimentary paleoenvironments: alluvial to tidal coastal flats. Characterised by channel incision and infileld by Seacliff Sandstone. Pronounced intrastratal deformation in the upper part of Reynella Siltstone Member. Major element chemical composition  shows evidence of salinization (high Na2O/K2O) and calcification (high CaO + MgO/Al2O3), but only modest chemical weathering (low alumina/bases and Ba/Sr). Correlable with Nuccaleena Formation.||Unit of Elatina Formation.||Overlain disconformably by Seacliff Sandstone. Underlain by Marino Arkose Member.|Fine-grained red rocks; silty. Thin clay seams metamorphosed to lower greenschist facies, sand; feldspar, micrite clasts, and siltstone peloids. Massive siltstones.|
16059|Reynella Siltstone Member|70334|5|Briefly described|p29,77|Neoproterozoic|Neoproterozoic|Geological province: Gawler Craton. Of Adelaide Geosyncline. Deposited during ice sheet retreat in the southwest Flinders and parts of the Mount Lofty Ranges.||Unit of Elatina Formation.|||Red-brown to purple-red massive siltstone and lithic siltstone.|
16059|Reynella Siltstone Member|70407|5|Briefly described|p103 Fig 2|Neoproterozoic|Neoproterozoic|Age: Marinoan.||Of Elatina Formation.||||
16059|Reynella Siltstone Member|71129|6|Mentioned|p118,123,127|Cryogenian|Cryogenian|Of Adelaide Geosyncline. Correlable to silty-shaly intervals in Whyalla Sandstone.||Unit of Elatina Formation.||||
16059|Reynella Siltstone Member|72247|5|Briefly described|p43|Neoproterozoic|Neoproterozoic|Of Adelaide Geosyncline.||Unit of Elatina Formation.||||
16059|Reynella Siltstone Member|72450|5|Briefly described|Brochure, Brochure map|||Product of an ice age ca. 600 Ma and is exposed north of Hallett Cove, along Christie Creek and Pedler Creek bicycle trail. Deformed by the Delamerian Orogeny.||Umberatana Group||Overlies the Wilmington Formation.|Massive red siltstone.|
16059|Reynella Siltstone Member|73188|5|Briefly described|p315-316, p326, p330|Neoproterozoic|Neoproterozoic|Mount Lofty Ranges.||Yerelina Subgroup, Umberatana Group|||Red siltstone with local glacial pebbles.|
16059|Reynella Siltstone Member|73227|6|Mentioned|p27|||||||||
16059|Reynella Siltstone Member|73236|4|Described|p34, p36-39, p47|Ediacaran[?]|Ediacaran[?]|Marinoan; represents Elatiana glaciation in the Adelaide area. Marine sedimentary rocks. Previously thought to be an in-faulted block of Sturt Tillite at Hallett Cove (Segnit, 1940). Erosive surface at base. Contains tidal rhythmites, granules, irregularly dolomitised intervals and rare small glacial clasts.|c. 640-635 Ma|Elatina Formation, Yerelina Subgroup, Umberatana Group, Heysen Supergroup||[Unconformably] overlain by Seacliff Sandstone (Sandison Subgroup, Wilpena Group).|Dark red siltstone, sandy to gritty in part, with dolomitic lenses and rare small pebbles.|
16067|Rhynie Sandstone|22869|6|Mentioned|P37|||||||||
16067|Rhynie Sandstone|22889|6|Mentioned|p31|Adelaidean|Adelaidean|Parent - Emeroo Subgroup.||||||
16067|Rhynie Sandstone|23557|5|Briefly described|p98|||Of Burra Group.||||||
16067|Rhynie Sandstone|23818|4|Described|p54|Adelaidean|Adelaidean|Max. thickness: 5000 ft. Basal unit of the Burra Group. Intertongues with the River Wakefield Group.||||||
16067|Rhynie Sandstone|24546|5|Briefly described|p2 - 3 Fig.2|Neoproterozoic|Neoproterozoic|Of Burra Group. Geological Province: Adelaide Fold Belt.||||||16-JAN-08
16067|Rhynie Sandstone|29780|4|Described|p21|||||||||
16067|Rhynie Sandstone|30801|6|Mentioned|p5|||Burra Group. Table p5-6.||||||29-AUG-18
16067|Rhynie Sandstone|30802|6|Mentioned|Table 1|||See also p13.||||||29-AUG-18
16067|Rhynie Sandstone|30807|6|Mentioned|p103|||Suggested map symbol||||||
16067|Rhynie Sandstone|31292|4|Described|p3|||Refers Wilson (1952) Equated with Aldgate Sst.||||||
16067|Rhynie Sandstone|32720|6|Mentioned|Table 1|||||||||
16067|Rhynie Sandstone|32722|6|Mentioned|Fig.3|||Adelaidean. Stromatolite||||||
16067|Rhynie Sandstone|32724|6|Mentioned|Fig.1|||Torrensian. Correlation||||||
16067|Rhynie Sandstone|32725|6|Mentioned|p2|||See also p3. Refers Wilson (1952)||||||29-AUG-18
16067|Rhynie Sandstone|33474|6|Mentioned|Fig.4|||||||||
16067|Rhynie Sandstone|33956|4|Described|p1040|||||||||
16067|Rhynie Sandstone|34521|5|Briefly described|p157|||Suitability for road-making||||||
16067|Rhynie Sandstone|34535|5|Briefly described|p54|||Torrensian.  See also p57, Fig.19||||||29-AUG-18
16067|Rhynie Sandstone|34536|6|Mentioned|Map legend|Adelaidean|Adelaidean|Torrensian||||||
16067|Rhynie Sandstone|34587|5|Briefly described|p36|||||||||
16067|Rhynie Sandstone|35090|6|Mentioned|Fig.1|||||||||
16067|Rhynie Sandstone|35255|6|Mentioned|Fig.6|||||||||
16067|Rhynie Sandstone|35270|6|Mentioned|p6|||||||||
16067|Rhynie Sandstone|35328|6|Mentioned|p9|||Stratigraphy||||||
16067|Rhynie Sandstone|36733|6|Mentioned|p23|||||||||
16067|Rhynie Sandstone|37461|5|Briefly described|p337|||See also Table 5.I||||||
16067|Rhynie Sandstone|37854|6|Mentioned|p13|||See Table 1.||||||
16067|Rhynie Sandstone|38068|6|Mentioned|p68|||||||||
16067|Rhynie Sandstone|38157|6|Mentioned|Table 1|||See also Table III.||||||
16067|Rhynie Sandstone|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Torrensian||||||
16067|Rhynie Sandstone|39352|6|Mentioned|Map legend|Adelaidean|Adelaidean|Torrensian||||||
16067|Rhynie Sandstone|40294|6|Mentioned|p9|||See also p32.||||||29-AUG-18
16067|Rhynie Sandstone|40695|6|Mentioned|p5|||||||||
16067|Rhynie Sandstone|41401|6|Mentioned|p32|||||||||
16067|Rhynie Sandstone|41403|6|Mentioned|p43|||||||||
16067|Rhynie Sandstone|41404|3|Fully described|p82|||||||||
16067|Rhynie Sandstone|42098|5|Briefly described|p51|||||||||
16067|Rhynie Sandstone|42222|6|Mentioned|p12|||||||||
16067|Rhynie Sandstone|42235|6|Mentioned|p136|||||||||
16067|Rhynie Sandstone|42813|6|Mentioned|p16|||||||||
16067|Rhynie Sandstone|43052|5|Briefly described|p177,Table 6.1|||Emeroo Subgroup||||||
16067|Rhynie Sandstone|44659|5|Briefly described|map legend|||Torrensian, lithology.||||||
16067|Rhynie Sandstone|44660|14|Not recorded|map legend|||Torrensian, lithology.||||||
16067|Rhynie Sandstone|44690|4|Described|map legend|||Geol. Atlas Series. (I/54-5). Unit of Burra Group. Torrensian.||||||
16067|Rhynie Sandstone|50327|6|Mentioned|p307|||Basal unit of Burra Group.||||||07-FEB-11
16067|Rhynie Sandstone|60958|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Fluvial sandstone and conglomerate with thin, red-brown siltstone interlayers. Geological Province: Adelaide Geosyncline.||||||14-APR-05
16067|Rhynie Sandstone|61121|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Fluvial sandstone and conglomerate with thin, red-brown siltstone interlayers.  Geological Province: Adelaide Geosyncline.||||||
16067|Rhynie Sandstone|62724|5|Briefly described|p22|Torrensian|Torrensian|Fluvial sediments preserved at Mootooroo Ridge. Geological Province: Olary Domain/Curnamona Province.||||||07-FEB-11
16067|Rhynie Sandstone|64793|5|Briefly described|p284 fig 3, p285|||Adelaide Rift Complex.||Basal unit of Burra Group.||||
16067|Rhynie Sandstone|64796|6|Mentioned|p183 fig 2, p191 Fig.9, p192, p184|Cryogenian|Cryogenian|Of Adelaide Rift Complex|777 +/- 7 Ma - age of underlying Boucaut Volcs.|Unit in Emeroo Subgroup.|||Alluvial fan (fluvial) sandstones.|29-AUG-18
16067|Rhynie Sandstone|65375|4|Described|p7, p25.|Neoproterozoic|Neoproterozoic|Sediments deposited along the Torrens Hinge Zone marginal to Adelaide Geosyncline. Thickness from <100m to >200m.|Deposited c.780 Ma.|Unit in Emeroo Subgroup.||Unconformably overlies Wallaroo Group basement. Is unconformably overlain by Sturt Tillite.|Mainly fluvial sandstone and conglomerate with thin red-brown siltstone interlayers.|
16067|Rhynie Sandstone|66522|5|Briefly described|p20 Fig.2, p22.|Neoproterozoic|Neoproterozoic|Clasts occur in the Skillogalee Dolomite-dominated breccia of the Burra Diapir, suggesting it has been emplaced from below.|Lower Adelaidean.|Unit in Burra Group.|||A 14 m wide megaclast in the Burra Diapir consists of medium- and coarse-grained feldspathic sandstone with heavy mineral cross-bedding.|
16067|Rhynie Sandstone|70405|6|Mentioned|p51 table 4|Neoproterozoic|Neoproterozoic|||Emeroo Subgroup||||
16067|Rhynie Sandstone|70819|5|Briefly described|p11, 13, 18-19|Neoproterozoic|Neoproterozoic|Clare Valley. Forms the ridge and hills to the west of the Valley.||Emeroo Subgroup.|Anama Siltstone Member.|Is overlain by/faulted against Skillogalee Dolomite. Is faulted against underlying Bungaree Quartzite/River Wakefield Formation/Blyth Dolomite.|Fluvial deposits.|
16067|Rhynie Sandstone|71237|14|Not recorded|p9, 18|||||||||
16067|Rhynie Sandstone|71239|14|Not recorded|p5, p9|||||||||
16067|Rhynie Sandstone|71240|2|Defined|p6, p9, p18|||||||Correlated with Aldgate Sst, Copley, Emeroo, Witchelina, Yendnalue Quartzites||
16067|Rhynie Sandstone|73110|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic||||||Sandstone, coarse-grained, feldspathic, conglomeratic.|
16067|Rhynie Sandstone|73188|6|Mentioned|p354|||Oldest unit exposed [in the region] west of the Clare-Spalding Fault and is folded into isoclinal folds with steep axial planes and in places near-vertical plunges.||||||
16067|Rhynie Sandstone|74367|5|Briefly described|p7 Fig.6, p8-9, p12-14, p18, p20|Tonian|Tonian||1513+/-26 Ma LA-ICP-MS detrital zircon MDA|Emeroo Subgroup||||
16110|Ripon Calcrete|23719|4|Described|p30|Pleistocene|Pleistocene|See also page 30 table 9. Geological Province: Gawler Craton. Max. thickness 1 m.||||||
16110|Ripon Calcrete|23818|5|Briefly described|p212 Fig.108, p213|Middle Pleistocene|Middle Pleistocene|Of the Bridgewater Formation.||||||
16110|Ripon Calcrete|29697|6|Mentioned|p22|||||||||
16110|Ripon Calcrete|29829|6|Mentioned|p178|||||||||
16110|Ripon Calcrete|30750|6|Mentioned|p1|||Middle Pleistocene age||||||
16110|Ripon Calcrete|30751|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
16110|Ripon Calcrete|30752|6|Mentioned|p4|||Developed during regression of sea P5.||||||
16110|Ripon Calcrete|30754|4|Described|p32|||Stratigraphic table P22||||||
16110|Ripon Calcrete|30758|6|Mentioned|p66|||Stratigraphy||||||
16110|Ripon Calcrete|30922|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
16110|Ripon Calcrete|31312|6|Mentioned|p70|||||||||
16110|Ripon Calcrete|31320|6|Mentioned|p15|||||||||
16110|Ripon Calcrete|31845|6|Mentioned|p6|||M.Pleistocene||||||
16110|Ripon Calcrete|31850|6|Mentioned|p39|||Refers Firman (1967,1969)||||||
16110|Ripon Calcrete|32419|6|Mentioned|p86|||||||||
16110|Ripon Calcrete|32432|6|Mentioned|Table 1|||||||||
16110|Ripon Calcrete|32458|6|Mentioned|p10|||||||||
16110|Ripon Calcrete|33055|6|Mentioned|Fig.1|||||||||
16110|Ripon Calcrete|33834|6|Mentioned|p16|||||||||
16110|Ripon Calcrete|34180|5|Briefly described|p215|||Middle Pleistocene||||||
16110|Ripon Calcrete|34536|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
16110|Ripon Calcrete|34758|6|Mentioned|Table 1|||||||||
16110|Ripon Calcrete|34831|6|Mentioned|p93|||||||||
16110|Ripon Calcrete|35097|6|Mentioned|Fig.4|||||||||
16110|Ripon Calcrete|35232|6|Mentioned|p15|||||||||
16110|Ripon Calcrete|35673|6|Mentioned|Fig.1|||Location plan, Para Hills quartzite quarry.||||||
16110|Ripon Calcrete|35772|4|Described|Table 1|||||||||
16110|Ripon Calcrete|36626|6|Mentioned|Fig.1|||||||||
16110|Ripon Calcrete|36834|6|Mentioned|Fig.1|||||||||
16110|Ripon Calcrete|37853|6|Mentioned|Fig.1|||||||||
16110|Ripon Calcrete|38068|6|Mentioned|p76|||||||||
16110|Ripon Calcrete|38107|6|Mentioned|p19|||See also P73||||||
16110|Ripon Calcrete|39349|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
16110|Ripon Calcrete|40219|6|Mentioned|p2|||||||||
16110|Ripon Calcrete|40442|5|Briefly described|p36|||||||||
16110|Ripon Calcrete|40941|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
16110|Ripon Calcrete|40942|6|Mentioned|p20|||||||||
16110|Ripon Calcrete|41619|6|Mentioned|Map legend|Pleistocene||||||||
16110|Ripon Calcrete|42138|6|Mentioned|p393|||||||||
16110|Ripon Calcrete|42292|5|Briefly described|p9|||See also Fig. 3 P12||||||
16110|Ripon Calcrete|42475|6|Mentioned|p23|||occurs within Bridgewater Formation, but not stratigraphically related.||||||
16110|Ripon Calcrete|42498|5|Briefly described|Map Legend|Pleistocene|Pleistocene|||||||
16110|Ripon Calcrete|42499|5|Briefly described|Map legend|Pleistocene||||||||
16110|Ripon Calcrete|42506|5|Briefly described|Map legend|Pleistocene||||||||
16110|Ripon Calcrete|42716|5|Briefly described|Map legend|Pleistocene||||||||
16110|Ripon Calcrete|42717|5|Briefly described|map legend|Pleistocene||||||||
16110|Ripon Calcrete|42738|5|Briefly described|map legend|Quaternary||||||||
16110|Ripon Calcrete|42966|3|Fully described|p214|||||||||
16110|Ripon Calcrete|43049|5|Briefly described|p26|||||||||
16110|Ripon Calcrete|43073|5|Briefly described|p16|||||||||
16110|Ripon Calcrete|44660|14|Not recorded|map legend||Pleistocene|Pleistocene, lithology.||||||
16110|Ripon Calcrete|44864|5|Briefly described|Map Legend||Pleistocene|||||||
16110|Ripon Calcrete|44935|5|Briefly described|Map Legend||Pleistocene|||||||
16110|Ripon Calcrete|62893|5|Briefly described|Map Legend, p24|Pleistocene|Pleistocene|Interbedded with Bridgewater Formation (Lower Member) including as a dense, very hard, pinkish calcrete cap.||||Equivalent to Lower Bridgewater Formation.|Nodular and sheet calcrete and carbonate cements.|
16110|Ripon Calcrete|65922|5|Briefly described|p25 Tb. 4, p27|Pleistocene|Pleistocene|Extensive and prominently developed hard massive sheet calcrete formed within Pleistocene deposits (including, commonly, Bridgewater Formation) in the Gawler Ranges.||||||
16110|Ripon Calcrete|70803|6|Mentioned|p56|||||||||
16110|Ripon Calcrete|73112|5|Briefly described|Map legend.|Pleistocene|Pleistocene|Calcrete of this unit and of the Bakara Soil is mapped as a single unit.|||||Forms a calcrete surface.|
16248|Rodda beds|22613|5|Briefly described|p16|Neoproterozoic|Neoproterozoic|||||||
16248|Rodda beds|22746|5|Briefly described|Fig.3 p515, p521|Neoproterozoic III|Neoproterozoic III|Equivalent of Ungoolya Group?||||||
16248|Rodda beds|23282|6|Mentioned|p59|||||||||12-JUL-07
16248|Rodda beds|23287|6|Mentioned|Fig.2,4|||Age: Lower Ediacarian. of Eastern Officer Basin.||||||
16248|Rodda beds|23288|6|Mentioned|p143 Fig.5|||||||||
16248|Rodda beds|24476|6|Mentioned|p547 Fig. 4|||Superseded by the Dey Dey Mudstone.||||||
16248|Rodda beds|40945|3|Fully described|p12|Paleoproterozoic|Paleoproterozoic|Redefinition. Age: Marinoan.||||||07-NOV-08
16248|Rodda beds|41833|6|Mentioned|p586|||||||||
16248|Rodda beds|42095|5|Briefly described|p31|||See also Fig.3||||||
16248|Rodda beds|42096|6|Mentioned|p36|||||||||
16248|Rodda beds|42816|4|Described|p13|||||||||
16248|Rodda beds|42940|5|Briefly described|p1|||||||||
16248|Rodda beds|43052|4|Described|p200,Table 6.2|||||||||
16248|Rodda beds|43650|5|Briefly described|p444|||||||||
16248|Rodda beds|43651|6|Mentioned|p440|||||||||
16248|Rodda beds|44109|5|Briefly described|p22 Fig. 19|Neoproterozoic|Neoproterozoic|Of the Ungoolya Group. Geological Province: central Officer Basin.||||||
16248|Rodda beds|44111|6|Mentioned|p.58 Fig. 2|||in Officer Basin, presented at "Rodda" only in Fig. 2.||||||
16248|Rodda beds|44133|5|Briefly described|p35|Neoproterozoic|Neoproterozoic|||||||
16248|Rodda beds|60565|5|Briefly described|p20 Fig. 3b|||Overlain by the Relief Sandstone. Overlies the Murnaroo Formation.||||||
16248|Rodda beds|60953|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Siltstone, often dolomitic or calcreous, calcareous sandstone, limestone and dolomite, often slumped.||||||
16248|Rodda beds|61108|5|Briefly described|map legend|Adelaidean|Adelaidean|Siltstone, often dolomitic or calcareous, calcareous sandstone, limestone and dolomite, commonly slumped.||||||
16248|Rodda beds|61565|6|Mentioned|p611|||Replaced by Dey Dey Mudstone. Geological Province: Officer Basin.||||||20-APR-06
16248|Rodda beds|61732|6|Mentioned|p61|||Name originally applied to outcrop north of Mount Johns (Krieg 1972, 1973). Later divided into several formations.||||||07-FEB-11
16248|Rodda beds|62570|5|Briefly described|p580 Fig. 2|||Of the Marla Group. Geological Province: Officer Basin.||||||01-OCT-09
16248|Rodda beds|63397|6|Mentioned|p5|Neoproterozoic|Neoproterozoic|||||||18-JUL-07
16248|Rodda beds|63811|6|Mentioned|p499|||Old term replaced by Ungoolya Group in Giles 1 area.||||||04-SEP-14
16248|Rodda beds|64797|6|Mentioned|p153 Fig.2|Ediacaran|Ediacaran|Officer Basin. Lithology/rank not shown on diagram.||||||
16248|Rodda beds|65376|6|Mentioned|p247 Fig.6.57.|Neoproterozoic|Neoproterozoic|||||||
16248|Rodda beds|65410|6|Mentioned|p74.|Neoproterozoic|Neoproterozoic|Officer Basin. Part of Supersequence 3. Contains distinctive, well-documented and well-constrained palynomorph assemblages of biostratigraphic significance, including acritarchs||||||
16248|Rodda beds|67536|6|Mentioned|Map Legend|||One of several Formations mapped collectively as N2.|||||Dominantly marine shale, siltstone, sandstone and limestone.|
16248|Rodda beds|67912|6|Mentioned|p13|||Previously included rocks now assigned to the Ungoolya Group.||||||
16248|Rodda beds|67921|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Shown only in section as (Rodda beds) and grouped with Punkerri Sandstone, Ungoolya Group. May be previous name for Ungoolya Group?||Of Ungoolya Group?||Said to be equivalent to Wilpena Group||
16248|Rodda beds|69438|6|Mentioned|p23:20|||Officer Basin.||||Correlated with Julie Formation (Amadeus Basin).||12-JUL-16
16248|Rodda beds|70336|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic||||||Grey-green khaki calcareous and dolomitic siltstone. Limestone and dolomite as allochthonous blocks.|
16248|Rodda beds|72478|6|Mentioned|Fig. 7 p70|||||||||
16248|Rodda beds|73086|6|Mentioned|p122, p124, p133|||Officer Basin. Large sphaeromorph and acanthomorph acritarch assemblages found in this unit; used to correlate with Pertatataka Formation.||||Correlates to Pertatataka Formation, Julie Formation.||
16248|Rodda beds|73090|5|Briefly described|p12 Fig.7, Appendix|Neoproterozoic|Neoproterozoic||||||Siltstone, grey-green, khaki calcareous and dolomitic, limestone and dolomite as allochthonous blocks.|
16248|Rodda beds|73100|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Subsurface. Appears as UNGOOLYA GROUP (RODDA BEDS). Alternative or previous name for Ungoolya Group?.||||Equivalent to Wilpena Group.||
16248|Rodda beds|73109|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Subsurface. Also referred to as Ungoolya Group.||||||
16248|Rodda beds|73111|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Subsurface. Appears as UNGOOLYA GROUP (RODDA BEDS).||||||
16248|Rodda beds|73392|6|Mentioned|p3||||||||Sampled from core of Munta 1 well.|
16251|Roe Calcarenite|23768|5|Briefly described|p27, p52, p65|Late Pliocene|Late Pliocene|Geological Province: Eucla Basin.  See also p30 Fig. 6 and p62-63.||||||
16251|Roe Calcarenite|24094|5|Briefly described|p273, p277|Late Pleistocene|Early Pleistocene|Thin, sandy limestone. Geological Province: Eucla Basin||||||16-MAR-05
16251|Roe Calcarenite|24347|5|Briefly described|p115 Fig.2|Pliocene|Pliocene|||||||
16251|Roe Calcarenite|31562|4|Described|p14|||Pleistocene||||||
16251|Roe Calcarenite|31903|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
16251|Roe Calcarenite|31908|4|Described|Table 1|||Pleistocene||||||
16251|Roe Calcarenite|31909|2|Defined|p9|Pleistocene|Pleistocene|||||||
16251|Roe Calcarenite|32552|2|Defined|p10|Quaternary|Quaternary|See also P23, 35, 81, 114 etc.||||||
16251|Roe Calcarenite|32648|6|Mentioned|p32|||Pleistocene||||||
16251|Roe Calcarenite|32750|4|Described|p306|||||||||
16251|Roe Calcarenite|34194|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
16251|Roe Calcarenite|35097|6|Mentioned|p15|||||||||
16251|Roe Calcarenite|35772|6|Mentioned|Table 1|||||||||
16251|Roe Calcarenite|36386|6|Mentioned|p156|||||||||
16251|Roe Calcarenite|36890|3|Fully described|p416|||||||||
16251|Roe Calcarenite|38553|6|Mentioned|p44|||||||||
16251|Roe Calcarenite|38699|6|Mentioned|p28|||||||||
16251|Roe Calcarenite|38700|6|Mentioned|p38|||||||||
16251|Roe Calcarenite|38774|6|Mentioned|p44|||||||||
16251|Roe Calcarenite|38982|6|Mentioned|p56|||||||||
16251|Roe Calcarenite|39522|6|Mentioned|p86|||||||||
16251|Roe Calcarenite|40992|6|Mentioned|Fig.23|||||||||
16251|Roe Calcarenite|41043|6|Mentioned|p87|||||||||
16251|Roe Calcarenite|41075|6|Mentioned|p32|||||||||
16251|Roe Calcarenite|41831|6|Mentioned|p556|||||||||
16251|Roe Calcarenite|42473|6|Mentioned|p15|||||||||
16251|Roe Calcarenite|43498|6|Mentioned|9||Pleistocene|||||||
16251|Roe Calcarenite|43667|6|Mentioned|Fig.3,p12||Pliocene|||||||
16251|Roe Calcarenite|44145|4|Described|p550 tab 4-27, p557-559|Pleistocene|Pliocene|Eucla Basin. Fossiliferous. Max thickness 8m.||||Disconformable on older rocks.|Weakly cemented, poorly bedded, medium to coarse grained, porous, shelly calcarenite: locally dolomitic.|
16251|Roe Calcarenite|61155|5|Briefly described|p5, p17|Pleistocene|Pliocene|Thin, very shallow-water calcarenites. Age: <2Ma. Geological Province:  Eucla Basin.||||||
16251|Roe Calcarenite|61517|5|Briefly described|p309|Late Pliocene|Pliocene|Bioclastic sandy limestone; richly fossiliferous, notably with mollusc shells. Unconformably overlies Wilson Bluff Limestone. Max. thickness: 7.5m.  Geological Province: Eucla Basin.||||||27-MAY-06
16251|Roe Calcarenite|62069|6|Mentioned|p108|Pliocene|Pliocene|In south Western Australia.||||||
16251|Roe Calcarenite|62369|3|Fully described|p407-4119|Early Pleistocene|Pliocene|Unlithified to friable lime sand, rich in macrofossils. Overlies the Abrakurrie Limestone and, locally, Wilson Bluff Limestone. Age: 2.6-1.8Ma (Sr-isotope). Geological Province: Eucla Basin; lies beneath the Roe Plains in the Great Australian Bight.||||||
16251|Roe Calcarenite|67472|5|Briefly described|180|Pliocene|Pliocene|Bioclastic limestone, Roe Plains. Includes new macrofossil gastropod species Notocypraea goudeyi.||||||11-JUL-13
16251|Roe Calcarenite|67789|5|Briefly described|p34, 41|Pliocene|Pliocene|Nullarbor Plain, Eucla Basin. Deposited during a sea level highstand event.||||Locally overlies Nullarbor Limestone.||
16251|Roe Calcarenite|70397|6|Mentioned|p2-3|Pleistocene|Pliocene|Eucla Basin. Warm-temperate seagrass bed deposits. Presently lies just above sea level, forming the surface of the Roe Plain.||||Underlain by Nullabor Limestone.||
16251|Roe Calcarenite|70771|4|Described|p3, p5, p7-p8, p11-p12, p32, |Pleistocene|Pliocene|Roe Plain, Eucla Basin. This highly fossiliferous unit contains fossilised molluscs (gastropods and bivalves), echinoids, benthic foraminifera and coralline algae. This unit was deposited uniformly on the Roe plain, covering approximately 8000 square kilometers at a thickness of 2-3m. Interpreted as the product of shallow marine, subtidal sedimentation in a seagrass dominated environment.  [The author assigns this unit to the Eucla Group however this term is obsolete]. See also p53-p58, p60-p61.||Eucla Group||Disconformably overlies the Wilson Bluff Limestone and the Abrakurrie Limestone.|Weakly lithified, coarse-grained, poorly-bedded and highly fossiliferous calc-arenite.|
16251|Roe Calcarenite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||biocarbonate, limestone, coastal sediment|
16251|Roe Calcarenite|71361|4|Described|p5, p15, p21, p67, p110|Early Pleistocene|Late Pliocene|Eucla Basin. Fossil assemblage includes benthic foraminifera, coralline algae and molluscs. Interpreted to have been deposited in a shallow, warm-temperate grass beds.||||Unconformably overlies the Nullarbor Limestone.|Unlithified fossiliferous Calc-arenite.|
16251|Roe Calcarenite|73084|6|Mentioned|p16|Pleistocene|Pliocene|||||||
16251|Roe Calcarenite|73641|5|Briefly described|p6 Fig.4|Pleistocene|Pliocene|Southern Eucla Basin.||||||
16267|Rolling Downs Group|730|6|Mentioned|p24, p25.|||Marine.||||||11-NOV-14
16267|Rolling Downs Group|9250|5|Briefly described|Map legend|Cretaceous|Cretaceous|Sandstone, siltstone and claystone., porcellaneous in part.||||||
16267|Rolling Downs Group|12575|5|Briefly described|p781. |Albian|Albian|Uppermost unit in Laura Basin. Vitrinite reflectance data are detailed.|124-97 Ma.||Includes Wollena Claystone.||Glauconitic open marine shale.|
16267|Rolling Downs Group|13516|5|Briefly described|p167 fig 10, p169 fig 11|Late Cretaceous|Early Cretaceous|In Surat Basin, Eromanga Basin.|||Includes Wilgunya Subgroup, Manuka Subgroup|||14-NOV-12
16267|Rolling Downs Group|22757|5|Briefly described|p7|||Also Table6, p11. Surat Basin.||||||28-NOV-06
16267|Rolling Downs Group|22780|5|Briefly described|map|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|22781|4|Described|p41|Early Cretaceous|Early Cretaceous|In the Carpentaria Basin.||||||02-APR-07
16267|Rolling Downs Group|22857|5|Briefly described|p294, p544 App.1 Tb.A1.12|Cenomanian|Aptian|Includes the Wallumbilla Formation, Surat Siltstone, Griman Creek Formation, and Winton Formation. Geological Province: Surat and Eromanga Basins. See also p296-7 Tb.22.1, p315 Fig. 22.8, p552 App.1 Tb.A1.13.||||||
16267|Rolling Downs Group|22865|4|Described|p294,Table22.1p296-7|Cenomanian|Aptian|||||||
16267|Rolling Downs Group|23053|4|Described|p8,11,28,30-1|Albian|Aptian|||||||
16267|Rolling Downs Group|23056|6|Mentioned|6|||Geological province: Eromanga Basin.||||||28-NOV-06
16267|Rolling Downs Group|23065|5|Briefly described|18|||Geological province: Carpentaria Basin.||||||28-NOV-06
16267|Rolling Downs Group|23183|6|Mentioned|p217||Aptian|||||||
16267|Rolling Downs Group|23220|6|Mentioned|p16|||||||||
16267|Rolling Downs Group|23224|5|Briefly described|p3|||Of McMinn 1981. Hosts the Wallumbilla Formation. Great Australian Basin.||||||07-MAR-06
16267|Rolling Downs Group|23291|4|Described|p80 Tb. 3.6|Early Cretaceous|Early Cretaceous|Age: Early Cretaceous. Conformably overlies Coffin Hill Member. Thickness: <10m. Geological Province: Georgetown Region.||||||26-NOV-08
16267|Rolling Downs Group|23336|5|Briefly described|p5|Cretaceous|Cretaceous|Overlies Mulga Downs Group.||||||28-NOV-06
16267|Rolling Downs Group|23393|5|Briefly described|p24|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|23420|6|Mentioned|p 131|||||||||
16267|Rolling Downs Group|23423|5|Briefly described|p267||Cretaceous|||||||
16267|Rolling Downs Group|23425|3|Fully described|p394 Table 9.7.|||Also see p378. Geological Province Carpentaria Basin.||||||03-APR-12
16267|Rolling Downs Group|23426|3|Fully described|p403 + Table 10.4 p407|Albian|Aptian|Formerly Battle Camp Shale and Wolena Claystone. Conformably underlain by Gilbert River Formation. Geological province: Laura Basin Province.||||||26-APR-07
16267|Rolling Downs Group|23427|5|Briefly described|Table 11.2 p418.|||||||||
16267|Rolling Downs Group|23428|5|Briefly described|p422|||||||||
16267|Rolling Downs Group|23430|5|Briefly described|p522|||Formerly Battle Camp Shale and Wolena Claystone. Basal shale is marine, variably calcareous and galuconitic, with minor siltstone and conglom. beds; overlain by marine silty/sandy claystone with calc.concretions. Geol. Prov: Laura Basin.||||||30-NOV-06
16267|Rolling Downs Group|23431|5|Briefly described|p544|||||||||
16267|Rolling Downs Group|23496|6|Mentioned|p59|||||||||
16267|Rolling Downs Group|23510|5|Briefly described|Map Legend||Early Cretaceous|||||||
16267|Rolling Downs Group|23511|5|Briefly described|Map Legend|Cretaceous|Middle Jurassic|||||||
16267|Rolling Downs Group|23512|5|Briefly described|Map Legend|Cretaceous|Middle Jurassic|||||||
16267|Rolling Downs Group|23518|5|Briefly described|p13|Mesozoic|Mesozoic|Geological Province: Carpentaria Basin.||||||
16267|Rolling Downs Group|23833|5|Briefly described|p256 Table 1|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|23879|6|Mentioned|p18|||||||||
16267|Rolling Downs Group|23883|5|Briefly described|p129 Fig. 11.2|Cretaceous|Cretaceous|Geological Province: Great Australian Superbasin.||||||
16267|Rolling Downs Group|23911|5|Briefly described|p97 Fig. 11|Albian|Aptian|Geological Province: Eromanga Basin.||||||
16267|Rolling Downs Group|23982|5|Briefly described|p2|Cretaceous|Cretaceous|Geological Province: Great Artesian Basin. See also page 35 Fig.7.||||||
16267|Rolling Downs Group|24047|5|Briefly described|p11-12|||Geological Province: Western Gulf Sub-basin.||||||
16267|Rolling Downs Group|24048|6|Mentioned|p76|||Geological Province: Carpentaria Basin.||||||
16267|Rolling Downs Group|24070|5|Briefly described|p303|Cretaceous|Cretaceous|Geological Province: Coonamble Embayment.||||||
16267|Rolling Downs Group|24073|5|Briefly described|p378 Table 2|Early Cretaceous|Early Cretaceous|Geological Province: Carpentaria Basin.||||||
16267|Rolling Downs Group|24089|5|Briefly described|Student Activites|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|24092|5|Briefly described|p8 Fig.3|||Geological Province: Eromanga Basin.||||||
16267|Rolling Downs Group|24243|5|Briefly described|p3 Fig.2|Cretaceous|Cretaceous|||||||
16267|Rolling Downs Group|24393|5|Briefly described|p152 Tb. 1|Mesozoic|Mesozoic|Shallow marine deposits <50m. thick.||||||
16267|Rolling Downs Group|29591|6|Mentioned|p69|||||||||
16267|Rolling Downs Group|29961|6|Mentioned|p12|||||||||
16267|Rolling Downs Group|29991|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
16267|Rolling Downs Group|30019|6|Mentioned|p2|||||||||
16267|Rolling Downs Group|30021|6|Mentioned|p87|||||||||
16267|Rolling Downs Group|30095|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|30102|5|Briefly described|p34|||Cretaceous age. See also p17.||||||28-NOV-06
16267|Rolling Downs Group|30103|5|Briefly described|p9|||Lower Cretaceous age. Table 3 on p9. See also Fig.2.||||||28-NOV-06
16267|Rolling Downs Group|30104|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|30133|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
16267|Rolling Downs Group|30510|6|Mentioned|p103|||||||||
16267|Rolling Downs Group|30582|6|Mentioned|p4|||||||||
16267|Rolling Downs Group|30584|4|Described|Table 1|||||||||
16267|Rolling Downs Group|30585|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|30587|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|30691|4|Described|p6|||See also p15-17,20,Table 4,Fig.2. Lower Cretaceous age.||||||28-NOV-06
16267|Rolling Downs Group|30692|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|30696|6|Mentioned|p16|||||||||
16267|Rolling Downs Group|30697|6|Mentioned|p34|||Minor aquifer present.||||||28-NOV-06
16267|Rolling Downs Group|30699|6|Mentioned|p53|||Stratigraphy. Early Cretaceous||||||
16267|Rolling Downs Group|30701|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|30702|4|Described|p48|||See also p51,52,Fig.1. Stratigraphic table.||||||28-NOV-06
16267|Rolling Downs Group|30853|5|Briefly described|Table 3|||Cretaceous||||||
16267|Rolling Downs Group|30854|4|Described|Table 4|||Lower to Upper Cretaceous age||||||
16267|Rolling Downs Group|30855|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
16267|Rolling Downs Group|30856|4|Described|Table 3|||Lower Cretaceous age||||||
16267|Rolling Downs Group|30857|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|30905|6|Mentioned|p147|||||||||
16267|Rolling Downs Group|30910|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
16267|Rolling Downs Group|30914|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
16267|Rolling Downs Group|31097|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|31098|5|Briefly described|Table 1|||||||||
16267|Rolling Downs Group|31109|6|Mentioned|p40|||See also P42, 44, 46, 50, 52, 54, 56, 58 & Map 62.||||||
16267|Rolling Downs Group|31110|5|Briefly described|p6|||See also p8-26. Terrain classification.||||||28-NOV-06
16267|Rolling Downs Group|31144|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower - Upper Cretaceous||||||
16267|Rolling Downs Group|31145|5|Briefly described|Table 1|||L. - U. Cretaceous||||||
16267|Rolling Downs Group|31164|6|Mentioned|p8|||Lower Cretaceous||||||
16267|Rolling Downs Group|31165|5|Briefly described|Table.1.|||||||||
16267|Rolling Downs Group|31166|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|31376|5|Briefly described|p4|||Mention p2.||||||28-NOV-06
16267|Rolling Downs Group|31422|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Includes the Wallumbilla Formation, Toolebuc Limestone and Allaru Mudstone.||||||02-DEC-04
16267|Rolling Downs Group|31425|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
16267|Rolling Downs Group|31430|4|Described|Table 1|||||||||
16267|Rolling Downs Group|31431|5|Briefly described|Table 3|||L.U.Cretaceous||||||
16267|Rolling Downs Group|31432|4|Described|Table 1|||L.Cretaceous||||||
16267|Rolling Downs Group|31433|5|Briefly described|p7|||Lower Cretaceous||||||
16267|Rolling Downs Group|31434|4|Described|Table 1|||Lower Cretaceous. See also p8.||||||28-NOV-06
16267|Rolling Downs Group|31436|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower Cretaceous - Upper Cretaceous||||||
16267|Rolling Downs Group|31437|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|31438|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|31440|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|31441|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower - Upper Cretaceous||||||
16267|Rolling Downs Group|31443|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|31553|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|32274|6|Mentioned|Map legend|Mesozoic|Mesozoic|||||||
16267|Rolling Downs Group|32275|4|Described|p8|||||||||
16267|Rolling Downs Group|32276|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|32277|6|Mentioned|Map legend|Mesozoic|Mesozoic|||||||
16267|Rolling Downs Group|32314|6|Mentioned|Fig.4|||||||||
16267|Rolling Downs Group|32392|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|32393|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|32395|6|Mentioned|p6|||Stratigraphic table.||||||28-NOV-06
16267|Rolling Downs Group|32396|6|Mentioned|p8|||L.Cretaceous||||||
16267|Rolling Downs Group|32413|6|Mentioned|p87|||||||||
16267|Rolling Downs Group|32563|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|32671|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
16267|Rolling Downs Group|32705|6|Mentioned|p183|||See also Fig.2||||||
16267|Rolling Downs Group|32706|4|Described|Table 1|||Mention p8.||||||28-NOV-06
16267|Rolling Downs Group|32796|4|Described|p301|||See also p302-303||||||28-NOV-06
16267|Rolling Downs Group|32918|4|Described|p18|||||||||11-JAN-10
16267|Rolling Downs Group|33011|6|Mentioned|p214|||||||||
16267|Rolling Downs Group|33016|6|Mentioned|p1|||||||||
16267|Rolling Downs Group|33017|6|Mentioned|p8|||||||||
16267|Rolling Downs Group|33067|4|Described|Table 1|Early Cretaceous|Early Cretaceous|Includes Winton, Mackunda and Wallumbilla Formations and Allaru Mudstone and Toolebuc Limestone.||||||07-JUL-04
16267|Rolling Downs Group|33068|6|Mentioned|p476|||Cret.||||||
16267|Rolling Downs Group|33069|4|Described|p7|||L.-U.Cret.||||||
16267|Rolling Downs Group|33070|4|Described|Table 2|||L.Cret.||||||
16267|Rolling Downs Group|33072|4|Described|Table 1|||L.Cret.||||||
16267|Rolling Downs Group|33073|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|33075|6|Mentioned|p452|||||||||
16267|Rolling Downs Group|33078|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower - Upper Cretaceous||||||
16267|Rolling Downs Group|33079|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower - Upper Cretaceous||||||
16267|Rolling Downs Group|33080|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|33082|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower - Upper Cretaceous||||||
16267|Rolling Downs Group|33083|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower - Upper Cretaceous||||||
16267|Rolling Downs Group|33086|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|33087|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
16267|Rolling Downs Group|33088|4|Described|Table 3|||L.Cret.||||||
16267|Rolling Downs Group|33089|4|Described|Table 2|||L.-U.Cret.||||||
16267|Rolling Downs Group|33090|4|Described|Table 4|||L.Cret.||||||
16267|Rolling Downs Group|33091|6|Mentioned|p9|||Strat.||||||
16267|Rolling Downs Group|33092|6|Mentioned|p8|||Strat. table||||||
16267|Rolling Downs Group|33094|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|33095|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|33096|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|33150|4|Described|p8|||L.Cret.||||||
16267|Rolling Downs Group|33151|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|33176|6|Mentioned|p175|||||||||
16267|Rolling Downs Group|33177|5|Briefly described|Table 1|||||||||15-JUL-04
16267|Rolling Downs Group|33178|5|Briefly described|p11|||||||||
16267|Rolling Downs Group|33181|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|33182|6|Mentioned|p193|||||||||
16267|Rolling Downs Group|33184|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|33185|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|33226|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|33372|6|Mentioned|Table 1|||||||||
16267|Rolling Downs Group|33448|4|Described|Table 1|||L.Cret.||||||11-JAN-10
16267|Rolling Downs Group|33449|4|Described|Table 1|||L.-U.Cret.||||||
16267|Rolling Downs Group|33451|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|33452|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|33528|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|33529|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|33561|6|Mentioned|p102|||||||||
16267|Rolling Downs Group|33638|5|Briefly described|Table 1|||See also p10.||||||28-NOV-06
16267|Rolling Downs Group|33639|5|Briefly described|p11|||L.Cret.||||||
16267|Rolling Downs Group|33640|4|Described|Table 2|||L.-U.Cret.||||||
16267|Rolling Downs Group|33642|6|Mentioned|p144,147,148|||Refers Vine & Day.(1965). Ref. to Whitehouse 1954. Subgroups. Ref to Jack 1886.||||||
16267|Rolling Downs Group|33643|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|33644|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|33646|5|Briefly described|p8|||Strat. table.||||||
16267|Rolling Downs Group|33647|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower - Upper? Cretaceous||||||
16267|Rolling Downs Group|33648|6|Mentioned|p19|||||||||
16267|Rolling Downs Group|33676|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
16267|Rolling Downs Group|33709|6|Mentioned|p110|||Cretaceous.||||||
16267|Rolling Downs Group|33772|4|Described|p13|||||||||
16267|Rolling Downs Group|33773|4|Described|Table 1|||||||||
16267|Rolling Downs Group|33825|6|Mentioned|p10|||Correlation table||||||
16267|Rolling Downs Group|33832|5|Briefly described|p11|||Strat. and correlation.||||||28-NOV-06
16267|Rolling Downs Group|33882|4|Described|Table 1|||Mention p7,8.||||||28-NOV-06
16267|Rolling Downs Group|33883|6|Mentioned|p17|||||||||
16267|Rolling Downs Group|33884|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|34065|4|Described|p6|||L.Cret.||||||
16267|Rolling Downs Group|34091|5|Briefly described|Table 1|||Cret. See also pp4,8.||||||28-NOV-06
16267|Rolling Downs Group|34174|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|34217|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower to Upper Cretaceous||||||
16267|Rolling Downs Group|34218|5|Briefly described|Table 1|||Lower Cretaceous.||||||28-NOV-06
16267|Rolling Downs Group|34254|6|Mentioned|p481|||||||||
16267|Rolling Downs Group|34282|6|Mentioned|p96|||Cret.||||||
16267|Rolling Downs Group|34287|6|Mentioned|p186|||Cret.||||||
16267|Rolling Downs Group|34469|6|Mentioned|p107|||Cretaceous. See also pp117,118.||||||28-NOV-06
16267|Rolling Downs Group|34487|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|34550|5|Briefly described|Table 2.1|||Cretaceous||||||
16267|Rolling Downs Group|34811|4|Described|Table 1|||||||||
16267|Rolling Downs Group|34931|5|Briefly described|p320|||||||||
16267|Rolling Downs Group|35187|6|Mentioned|p53|||||||||
16267|Rolling Downs Group|35204|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|35220|4|Described|p16|||||||||
16267|Rolling Downs Group|35253|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|35559|4|Described|Table 1|||||||||
16267|Rolling Downs Group|35560|6|Mentioned|p289|||||||||
16267|Rolling Downs Group|35601|6|Mentioned|p144|||Geothermal gradients correlate with contours of base of R.D.Group||||||
16267|Rolling Downs Group|35640|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|35663|6|Mentioned|Table 1|||Biostratigraphy.||||||
16267|Rolling Downs Group|35793|6|Mentioned|p241|||Weathered profiles.||||||
16267|Rolling Downs Group|35811|5|Briefly described|Table 3|||||||||
16267|Rolling Downs Group|35855|6|Mentioned|Fig.2|||Early Cretaceous lithostratigraphy.||||||
16267|Rolling Downs Group|36012|3|Fully described|Table 5|||||||||
16267|Rolling Downs Group|36056|6|Mentioned|p11|||||||||
16267|Rolling Downs Group|36228|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|36229|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|36473|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
16267|Rolling Downs Group|36570|6|Mentioned|p46|||||||||
16267|Rolling Downs Group|36571|6|Mentioned|Table 4|||||||||
16267|Rolling Downs Group|36751|6|Mentioned|p488|||||||||
16267|Rolling Downs Group|36910|6|Mentioned|p61|||||||||
16267|Rolling Downs Group|36914|6|Mentioned|p87|||||||||
16267|Rolling Downs Group|36961|6|Mentioned|Table 1|||||||||
16267|Rolling Downs Group|37116|6|Mentioned|p310|||||||||
16267|Rolling Downs Group|37608|3|Fully described|Table 1|||See also Table 2||||||
16267|Rolling Downs Group|37995|4|Described|Table 1|||||||||
16267|Rolling Downs Group|38064|5|Briefly described|p42|||Contain opal deposits of White Cliffs and Lightning Ridge.||||||
16267|Rolling Downs Group|38226|6|Mentioned|Table 1|||||||||
16267|Rolling Downs Group|38374|6|Mentioned|p602|||||||||
16267|Rolling Downs Group|39211|6|Mentioned|p5|||Fig. 3,7,9,22,26 etc. Correlation||||||
16267|Rolling Downs Group|39315|6|Mentioned|Fig.5|||||||||
16267|Rolling Downs Group|39445|5|Briefly described|Table 11|||||||||
16267|Rolling Downs Group|39478|6|Mentioned|Table 1|||||||||
16267|Rolling Downs Group|39494|6|Mentioned|Fig.5|||||||||
16267|Rolling Downs Group|39556|5|Briefly described|Map legend|Cretaceous|Cretaceous|||||||
16267|Rolling Downs Group|39627|6|Mentioned|p269|||||||||
16267|Rolling Downs Group|39666|6|Mentioned|p110|||||||||
16267|Rolling Downs Group|39708|6|Mentioned|p478|||||||||
16267|Rolling Downs Group|39899|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
16267|Rolling Downs Group|39942|6|Mentioned|p468|||||||||
16267|Rolling Downs Group|40030|6|Mentioned|Fig.5|||||||||
16267|Rolling Downs Group|40199|6|Mentioned|Fig.2|||||||||
16267|Rolling Downs Group|40544|6|Mentioned|Fig.6|||||||||
16267|Rolling Downs Group|40584|6|Mentioned|p434|||||||||
16267|Rolling Downs Group|40595|6|Mentioned|Fig.7|||||||||
16267|Rolling Downs Group|40623|5|Briefly described|p88|||||||||
16267|Rolling Downs Group|40648|3|Fully described|p12|||||||||
16267|Rolling Downs Group|40766|5|Briefly described|p25|||||||||
16267|Rolling Downs Group|40801|6|Mentioned|p79|||||||||
16267|Rolling Downs Group|40926|6|Mentioned|Table 2|||||||||
16267|Rolling Downs Group|41012|6|Mentioned|p137|||||||||
16267|Rolling Downs Group|41022|6|Mentioned|p279|||||||||
16267|Rolling Downs Group|41061|6|Mentioned|p19|||See also Fig.6. Generalized stratigraphy.||||||28-NOV-06
16267|Rolling Downs Group|41064|6|Mentioned|p55|||||||||
16267|Rolling Downs Group|41086|3|Fully described|p98|||See also Fig.3||||||
16267|Rolling Downs Group|41087|6|Mentioned|Fig.2|||||||||
16267|Rolling Downs Group|41088|6|Mentioned|p143|||||||||
16267|Rolling Downs Group|41097|6|Mentioned|Table 1|||||||||
16267|Rolling Downs Group|41117|6|Mentioned|Fig.2|||||||||
16267|Rolling Downs Group|41177|6|Mentioned|Fig.2|||||||||
16267|Rolling Downs Group|41188|6|Mentioned|Fig.3|||||||||
16267|Rolling Downs Group|41210|5|Briefly described|Fig.3|||||||||
16267|Rolling Downs Group|41247|6|Mentioned|Fig.7|||||||||
16267|Rolling Downs Group|41266|6|Mentioned|Fig.3|||||||||
16267|Rolling Downs Group|41307|4|Described|p17|||||||||
16267|Rolling Downs Group|41568|4|Described|p15|||||||||
16267|Rolling Downs Group|41642|6|Mentioned|p217|||||||||
16267|Rolling Downs Group|41681|6|Mentioned|p2|||||||||
16267|Rolling Downs Group|41725|6|Mentioned|Fig.2|||||||||
16267|Rolling Downs Group|41992|4|Described|Fig.2 P183|||See also p186.||||||28-NOV-06
16267|Rolling Downs Group|42007|6|Mentioned|Fig.2 P182|||||||||
16267|Rolling Downs Group|42061|5|Briefly described|Fig.4 P151|||||||||
16267|Rolling Downs Group|42121|6|Mentioned|Fig.1 P97|||||||||
16267|Rolling Downs Group|42346|4|Described|p81, Fig.4 p82|Early Cretaceous||||||||
16267|Rolling Downs Group|42364|5|Briefly described|Fig. 1 P196|||||||||
16267|Rolling Downs Group|42460|5|Briefly described|Fig.1 P206|||||||||
16267|Rolling Downs Group|42464|6|Mentioned|p8|||||||||
16267|Rolling Downs Group|42467|5|Briefly described|Map Legend|||||||||
16267|Rolling Downs Group|42596|5|Briefly described|Fig. 1 P24|||||||||
16267|Rolling Downs Group|42637|5|Briefly described|p10, 23|||||||||
16267|Rolling Downs Group|42650|4|Described|p16|||Conformably overlies/overlaps the Gilbert River Formation.||||||28-NOV-06
16267|Rolling Downs Group|42653|5|Briefly described|p318|||Terrain pattern description||||||
16267|Rolling Downs Group|42673|6|Mentioned|p195|||||||||
16267|Rolling Downs Group|43000|5|Briefly described|Fig.5,p112|||||||||
16267|Rolling Downs Group|43085|6|Mentioned|p8|||||||||
16267|Rolling Downs Group|43090|5|Briefly described|Map legend||Cretaceous|||||||
16267|Rolling Downs Group|43276|5|Briefly described|Map Legend||Early Cretaceous|||||||
16267|Rolling Downs Group|43277|5|Briefly described|Map Legend||Early Cretaceous|In the Great Australian Basin.||||||28-NOV-06
16267|Rolling Downs Group|43366|14|Not recorded|Map Legend|||||||||22-DEC-09
16267|Rolling Downs Group|43367|14|Not recorded|Map Legend|||||||||11-JAN-10
16267|Rolling Downs Group|43368|14|Not recorded|Map Legend|||||||||
16267|Rolling Downs Group|43369|14|Not recorded|Map Legend|||||||||
16267|Rolling Downs Group|43371|14|Not recorded|Map Legend|||||||||11-JAN-10
16267|Rolling Downs Group|43383|14|Not recorded|p26-28, diag||Cretaceous|||||||
16267|Rolling Downs Group|43384|14|Not recorded|Map Legend||Cretaceous|||||||
16267|Rolling Downs Group|43386|14|Not recorded|Map Legend||Cretaceous|||||||
16267|Rolling Downs Group|43390|14|Not recorded|p15,16,27-34|||Divided into Winton,Tambo,Roma Formations||||||
16267|Rolling Downs Group|43402|14|Not recorded|Map Legend||Cretaceous|||||||
16267|Rolling Downs Group|43403|14|Not recorded|Map Legend||Cretaceous|||||||
16267|Rolling Downs Group|43404|14|Not recorded|p11-15,20,23-33||Cretaceous|Table p9,Table p11||||||
16267|Rolling Downs Group|43405|14|Not recorded|Map Legend||Cretaceous|(Provisional Edition)||||||
16267|Rolling Downs Group|43410|14|Not recorded|Map Legend||Cretaceous|(Provisional Edition)||||||
16267|Rolling Downs Group|43411|14|Not recorded|Map Legend|||||||||
16267|Rolling Downs Group|43436|14|Not recorded|Map Legend||Cretaceous|(Provisional Edition)||||||
16267|Rolling Downs Group|43452|5|Briefly described|Map Legend||Cretaceous|Includes: Roma Formation, Tambo Formation, Winton Formation.||||||14-FEB-05
16267|Rolling Downs Group|43454|14|Not recorded|Map Legend||Cretaceous|||||||
16267|Rolling Downs Group|43459|14|Not recorded|p315-6|||||||||
16267|Rolling Downs Group|43487|5|Briefly described|20|||||||||
16267|Rolling Downs Group|43501|14|Not recorded|Map Legend||Cretaceous|(Provisional Edition) Inc. Yalpunga Beds, Oornoo Beds, Wittabrenna Beds||||||
16267|Rolling Downs Group|43542|14|Not recorded|Map Legend||Cretaceous|lithology||||||
16267|Rolling Downs Group|43596|4|Described|p40, p39 Tb. 4|Albian|Aptian|Max. thickness: 600m. Largely comprises mudstone, with beds and lenses of glauconitic, labile, white to buff quartzose fine sandstone; fossiliferous and with  concretionary limestone at base; shallow marine deposits.||||||15-JAN-09
16267|Rolling Downs Group|43602|5|Briefly described|Fig3 p194|||In Surat Basin/Eromanga Basin||||||
16267|Rolling Downs Group|43625|6|Mentioned|p47|||||||||
16267|Rolling Downs Group|43630|6|Mentioned|p69|||||||||
16267|Rolling Downs Group|43714|6|Mentioned|p8||Early Cretaceous|||||||
16267|Rolling Downs Group|43730|5|Briefly described|p24,29|||||||||
16267|Rolling Downs Group|43738|6|Mentioned|p5|||||||||
16267|Rolling Downs Group|43810|6|Mentioned|Fig.4,p209,210||Cretaceous|||||||
16267|Rolling Downs Group|43820|5|Briefly described|Map Legend||Early Cretaceous|||||||
16267|Rolling Downs Group|43881|14|Not recorded|p79,80|Cretaceous|Late Jurassic|See also Lexicon.||||||
16267|Rolling Downs Group|43995|14|Not recorded|Tb.p9,20 Fig.9||Cretaceous|Inc. Roma Formation, Tambo Formation and Winton Formation in the Eromanga Sub-Basin.||||||
16267|Rolling Downs Group|44020|14|Not recorded|p10,Tb.1|Late Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|44033|14|Not recorded|Tb.1,opp.p4|||||||||
16267|Rolling Downs Group|44034|6|Mentioned|Tb.1,p2|||||||||
16267|Rolling Downs Group|44041|6|Mentioned|Fig.1|||||||||
16267|Rolling Downs Group|44087|14|Not recorded|p4|||||||||
16267|Rolling Downs Group|44089|14|Not recorded|Tb.1||Early Cretaceous|||||||
16267|Rolling Downs Group|44091|14|Not recorded|p60||Cretaceous|||||||
16267|Rolling Downs Group|44093|6|Mentioned|p68 (photo)|||Associated with Gum Vale beds.||||||
16267|Rolling Downs Group|44099|14|Not recorded|Map Legend|Late Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|44112|6|Mentioned|p82|||||||||
16267|Rolling Downs Group|44121|14|Not recorded|p8|||||||||
16267|Rolling Downs Group|44122|14|Not recorded|p322|||||||||
16267|Rolling Downs Group|44207|14|Not recorded|p116|||||||||
16267|Rolling Downs Group|44269|14|Not recorded|p16||Cretaceous|||||||
16267|Rolling Downs Group|44291|14|Not recorded|p5|||||||||
16267|Rolling Downs Group|44346|14|Not recorded|p4|||||||||
16267|Rolling Downs Group|44375|14|Not recorded|p313|||||||||
16267|Rolling Downs Group|44406|14|Not recorded|p4|||||||||
16267|Rolling Downs Group|44408|14|Not recorded|p4|||||||||
16267|Rolling Downs Group|44415|14|Not recorded|p22,Fig.2,p23|||||||||
16267|Rolling Downs Group|44417|2|Defined|p417-421|Albian|Aptian|Contains: Winton, Mackunda and Wilgunya Formations. Overlies Gilbert River Formation. Probably Cenomanian.||||||
16267|Rolling Downs Group|44739|14|Not recorded|p19|||||||||
16267|Rolling Downs Group|44740|14|Not recorded|p29,39-42,47,48,52,|||p55,56,77||||||
16267|Rolling Downs Group|44744|14|Not recorded|p106-113|||||||||
16267|Rolling Downs Group|44800|14|Not recorded|p16,22,map||Cretaceous|||||||
16267|Rolling Downs Group|44819|14|Not recorded|p89|Albian|Aptian|Shaley basal formation is Roma Formation.||||||
16267|Rolling Downs Group|44836|14|Not recorded|p5,11,Figs.1-5||Cretaceous|||||||
16267|Rolling Downs Group|44852|14|Not recorded|p78||Early Cretaceous|||||||
16267|Rolling Downs Group|44989|14|Not recorded|p.125,126|||(E54-14).||||||
16267|Rolling Downs Group|45004|14|Not recorded|p.8|||Tb.1.||||||
16267|Rolling Downs Group|45011|14|Not recorded|p18,20|||Whitehouse correlated sediments in Polland Shale with Rolling Downs Group.||||||
16267|Rolling Downs Group|45110|6|Mentioned|p6|||||||||
16267|Rolling Downs Group|45145|3|Fully described|Table 5|||See also p23.||||||31-OCT-06
16267|Rolling Downs Group|46791|4|Described|p44|||Refers Galloway (1967)||||||
16267|Rolling Downs Group|46802|6|Mentioned|p131|||||||||
16267|Rolling Downs Group|46812|5|Briefly described|p241|||||||||
16267|Rolling Downs Group|46854|6|Mentioned|Fig.1|||||||||
16267|Rolling Downs Group|46872|6|Mentioned|p108|||||||||
16267|Rolling Downs Group|46881|6|Mentioned|Table 2|||||||||
16267|Rolling Downs Group|46911|6|Mentioned|Fig.1|||Geological map and distribution of weathered profiles.||||||
16267|Rolling Downs Group|46937|6|Mentioned|Fig.10|||||||||
16267|Rolling Downs Group|46939|6|Mentioned|Fig.1|||||||||
16267|Rolling Downs Group|47042|6|Mentioned|p171|||||||||
16267|Rolling Downs Group|47083|5|Briefly described|p20||Mesozoic|Carpentaria Basin.||||||
16267|Rolling Downs Group|48908|14|Not recorded|Tb.1||Cretaceous|||||||
16267|Rolling Downs Group|48920|3|Fully described|p56|||Cretaceous||||||
16267|Rolling Downs Group|48951|6|Mentioned|Table 1|||||||||
16267|Rolling Downs Group|50100|5|Briefly described|p23|Cretaceous|Cretaceous|Comprises Wallumbilla and Toolebuc Formations, Allaru Mudstone and Mackunda Formation.  Overlies the Gilbert River Formation.  Geological Province:  Eromanga Basin.||||||
16267|Rolling Downs Group|60087|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Includes Allaru Mudstone, Toolebuc Limestone, and Wallumbilla Formation.||||||
16267|Rolling Downs Group|61312|5|Briefly described|p66, p73|Albian|Aptian|Supersedes "Rolling Downs Formation". Comprises Wallumbilla and Toolebuc Formations, and Allaru Mudstone and Winton Formation. Geological Province: Eromanga Basin.||||||
16267|Rolling Downs Group|61377|5|Briefly described|p148 Tb. SU1|Early Cretaceous|Early Cretaceous|Includes the Griman Creek Formation, Surat Siltstone and Wallumbilla Formation. Green silty mudstone, minor sandstone. Geological Province: Surat Basin. See also p149 Fig. SU8.||||||07-FEB-11
16267|Rolling Downs Group|61823|5|Briefly described|p118|||Part of a marine transgressive sequence; overlies Gum Vale and Cadna-Owie Formations. Geological Province: Eromanga Basin.||||||
16267|Rolling Downs Group|62837|5|Briefly described|Stratigraphic columns|Late Cretaceous|Early Cretaceous|Includes Wallumbilla Formation, Allaru Mudstone and Normanton Formation.  Age: ~114-91Ma. Geological Province: Northern Gulf of Carpentaria, Southern Cape York and Burketown Depression.||||||01-MAR-10
16267|Rolling Downs Group|63450|5|Briefly described|p83|Cretaceous|Jurassic|Overlies Hooray Sandstone/Cadna-owie Formation. Marine deposits.||||||07-FEB-11
16267|Rolling Downs Group|63789|5|Briefly described|Map Legend|Cretaceous|Late Jurassic|Includes Hooray Sandstone. Subaerial scree and slope debris deopsits on fossil hill slopes and valley walls containing dislodged angular blocks of underlying bedrock. Commonly with pebbly sand infill and silcrete cement.||||||08-DEC-08
16267|Rolling Downs Group|63790|5|Briefly described|Map Legend|Cretaceous|Late Jurassic|Includes Hooray Sandstone. Beach pebble, cobble and boulder deposits formed from white quartzose sandstone. Commonly with silcrete cement.||||||08-DEC-08
16267|Rolling Downs Group|63793|6|Mentioned|p10.|Cretaceous|Jurassic|Eromanga Basin.||||||
16267|Rolling Downs Group|63979|6|Mentioned|p51-52|||Includes the Wilgunyah Subgroup.||||||07-FEB-11
16267|Rolling Downs Group|64061|6|Mentioned|p66|Cretaceous|Cretaceous|Contains the Griman Creek Formation. Geological Province: Surat Basin.||||||24-APR-08
16267|Rolling Downs Group|64570|5|Briefly described|p858|Early Cretaceous|Early Cretaceous|Volcanogenic sedimentary rocks and are rich in volcanic lithics.||||||22-DEC-08
16267|Rolling Downs Group|64665|5|Briefly described|p53 Fig.2, p62.|Early Cretaceous|Early Cretaceous|Laura Basin.||||Overlies Gilbert River Formation.|Dominantly marine shales and siltstones.|
16267|Rolling Downs Group|64679|5|Briefly described|Map legend|Cretaceous|Cretaceous|Conglomerate (pebbles of rounded white vein quartz and quartzite), quartz sandstone, siltstone and claystone; commonly silicified or ferruginised.||||||27-NOV-08
16267|Rolling Downs Group|64681|5|Briefly described|p2, p3 Fig. 1|Cretaceous|Cretaceous|Geological province: Eromanga Basin. Sandstone, siltstone, claystone.||||||
16267|Rolling Downs Group|64682|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|Feldspathic and lithic sandstone, siltstone and mudstone; strongly kaolinised, mottled and ferruginised, locally containes exotic ?drop? boulders.||||||
16267|Rolling Downs Group|64683|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Includes Hooray Sandstone. Rounded waterworn white vein quartz and quartzite conglomerate, quartzose sandstones, siltstones and claystones deposited on undulating topography in underlying bedrock.||||||
16267|Rolling Downs Group|64820|4|Described|pS9, pS6 Fig. 4|Late Cretaceous|Middle Jurassic|Contains Garroway Sandstone, Gilbert River, Wallumbilla and Toolbeuc Formations, Allaru Mudstone and Normanton Formation. Overlain by Bulimba Formation.||||||
16267|Rolling Downs Group|64821|5|Briefly described|pS18, pS20-21, pS40|Cretaceous|Cretaceous|Discussed in relation to its saprolite zone in the East Weipa and Andoom areas where lenses of weakly lithified sandstone, clay and siltstone dominate. Unconformably overlain by the Bulimba Formation.||||||02-FEB-09
16267|Rolling Downs Group|64822|5|Briefly described|pS88, pS99|||Together with the overlying Bulimba Fm, hosted the development of the Weipa bauxite deposit - composed of a transported blanket of bauxite overlying a lateritic weathering profile. Geol.prov: Weipa Sub-basin, Carpentaria Basin.||||||02-FEB-09
16267|Rolling Downs Group|66529|6|Mentioned|p12 Fig.5|||Eromanga, Carpentaria, Surat Basins and Coonamble Embayment.|||Includes Wallumbilla, Toolebuc, Mackunda, Winton, Griman Creek Formations; Surat Siltstone; and Allaru Mudstone.|||
16267|Rolling Downs Group|66623|3|Fully described|p108, pp238-245, pp256-267.|Late Cretaceous|Early Cretaceous|Widespread throughout Eromanga Basin. Thickness c.600 m. Generally poor outcrops. Has fair hydrocarbon reservoir (no source) potential, and good local seal potential. Porous sandstone units provide groundwater resources.|||Includes Wilgunya Subgroup (in Queensland), Wallumbilla Formation (at base), Allaru Mudstone and Winton Formation (at top).|Overlies Cadna-owie Formation. Is unconformably overlain by Eyre Formation. Unconformably overlies Yancannia Formation.|Alternation of sandstone-poor and sandstone-rich intervals deposited in a marine environment; ice-rafted dropstone boulders in lower units.|07-JUN-13
16267|Rolling Downs Group|66915|5|Briefly described|p4-5, p15-17|||In later Rolling Downs Group units, the Toolebuc Formation is the only distinct and laterally persistent seismic reflection for correlation and is widespread in the Eromanga Basin.|||Wallumbilla Formation, Toolebuc Formation|||12-JAN-17
16267|Rolling Downs Group|66917|5|Briefly described|Map legend|Cretaceous|Cretaceous||||Includes Namur Sandstone.||Rounded, waterworn, white vein quartz, quartzite, conglomerate, quartzose sandstones, siltstones and claystones; overall upward-fining sequence with sparse marine fossils and large, rounded, quartzite dropstones.|
16267|Rolling Downs Group|66918|5|Briefly described|Map legend|Cretaceous|Cretaceous||||||Rounded, waterworn, white vein quartz and quartzite; conglomerate; quartzose sandstone; siltstones and claystones; overall upward-fining sequence with sparse marine fossils and large, rounded quartzite dropstones.|
16267|Rolling Downs Group|66920|5|Briefly described|Map legend|Cretaceous|Cretaceous||||Includes Wallumbilla Formation.||Rounded, waterworn, white vein quartz, quartzite, conglomerate, quartzose sandstones, siltstones and claystones; overall upward-fining sequence with sparse marine fossils and large, rounded, quartzite dropstones.|
16267|Rolling Downs Group|66921|6|Mentioned|Map legend|Cretaceous|Cretaceous||||Includes Cadna-owie Formation.|||
16267|Rolling Downs Group|67105|6|Mentioned|p661|Cretaceous|Cretaceous|||||||
16267|Rolling Downs Group|67207|5|Briefly described|Map legend.|Cretaceous|Cretaceous||||Includes Wallumbilla Formation.||Rounded, waterworn, white vein quartz, quartzite, conglomerate, quartzose sandstones, siltstones and claystones; overall upward-fining sequence with sparse marine fossils and large, rounded quartzite dropstones.|
16267|Rolling Downs Group|67208|5|Briefly described|Map legend.|Cretaceous|Cretaceous||||||Rounded, waterworn, white vein quartz, quartzite, conglomerate, quartzose sandstones, siltstones and claystones; overall upward-fining sequence with sparse marine fossils and large, rounded quartzite dropstones.|
16267|Rolling Downs Group|67209|5|Briefly described|Map legend.|Cretaceous|Cretaceous||||Includes Wallumbilla Formation and Allaru Mudstone.|Overlies Cadna-owie Formation. Is overlain by Cordillo Silcrete.|Rounded, waterworn, white vein quartz, quartzite, conglomerate, quartzose sandstones, siltstones and claystones; overall upward-fining sequence with sparse marine fossils and large, rounded, quartzite dropstones.|
16267|Rolling Downs Group|67210|5|Briefly described|Map legend.|Cretaceous|Cretaceous|||||Overlies Yancannia Formation. Unconformably overlies Warratta Group. Is overlain by Eyre Formation.|Marine white claystones, siltstones and fine-grained quartzose sandstones with bioturbation.|
16267|Rolling Downs Group|67211|5|Briefly described|Map legend.|Cretaceous|Cretaceous||||Includes Wallumbilla Formation and Allaru Mudstone.|Overlies Bunker Creek Formation and Warratta Group.|Rounded, waterworn, white vein quartz, quartzite, conglomerate, quartzose sandstones, siltstones and claystones; overall upward-fining sequence with sparse marine fossils and large, rounded, quartzite dropstones.|
16267|Rolling Downs Group|67402|4|Described|p179, p226-p230, p232, p309|Cenomanian|Aptian|Proven hydrocarbon seal in the Eromanga Basin with a combined thickness of up to 1500m; also present in the Laura Basin. Formerly the Battle Camp Shale and the Wolena Claystone.|||Includes the Allaru Mudstone, Toolebuc Formation and the Wallumbilla Formation|Overlies the Gilbert River Formation|Basal shale with minor silty and conglomeratic beds that is overlain by silty or sandy claystone with calcareous concretions.|
16267|Rolling Downs Group|67669|5|Briefly described|p11|Early Cretaceous|Early Cretaceous|Of Bowen Basin.|||Includes Wallumbilla Formation.|Underlain by Blythesdale Group.||
16267|Rolling Downs Group|68003|5|Briefly described|p52, p57 Fig.3-n, pp70-71, p127.|Early Cretaceous|Early Cretaceous|Surat Basin. Deposited in a major marine transgression-regression cycle.|||Includes Wallumbilla Formation, Surat Siltstone and Griman Creek Formation.|Overlies Bungil Formation and Drildool beds conformably.|Semiconsolidated clays and claystone with minor fine clayey quartz sandstone; coal and calcareous clay and calcarenite occur near the base; rare conglomerate and gravel.|
16267|Rolling Downs Group|68004|6|Mentioned|p131, p205.|Early Cretaceous|Early Cretaceous|Hosts the Lightning Ridge Opal Field. Mineral potential tracts and levels of certainty are discussed.||||||
16267|Rolling Downs Group|68069|5|Briefly described|Map legend, p2.|Cretaceous|Cretaceous|Surat Basin.|||Includes Wallumbilla Formation, Surat Siltstone and Griman Creek Formation.|||
16267|Rolling Downs Group|68553|6|Mentioned|Map legend; schematic diagram.|Cretaceous|Cretaceous|Surat, Laura, Carpentaria and Eromanga Basins.|||Includes Wallumbilla, Griman Creek, Toolebuc, Normanton, Mackunda and Winton Formations, and Allaru Mudstone.|||
16267|Rolling Downs Group|68593|5|Briefly described|p3-4|Early Cretaceous|Early Cretaceous|See individual units.|||Purlawaugh, Griman Creek Formations; Surat Siltstone.|Overlies Bungil Formation.||
16267|Rolling Downs Group|68734|5|Briefly described|p218 Fig.2|Albian|Barremian|Eromanga Basin (SW and NE) and Surat Basin.|||Includes Winton, Mackunda, Oodnadatta, Toolebuc, Wallumbilla, and Griman Creek Formations; Coorikiana Sandstone; Bulldog Shale; Allaru Mudstone; and Surat Siltstone.|||16-JAN-17
16267|Rolling Downs Group|68821|5|Briefly described|p292 Fig.1, p295|Cretaceous|Cretaceous|Lower Cretaceous age. Includes both marine and fluvial sedimentary rocks. Thick fluvial to coastal plain sequence.|||Includes Winton Formation, Mackunda Formation, Griman Creek Formation, Allaru Formation, Toolebuc Formation, Surat Siltstone, and Bulldog Shale.||Comprises carbonaceous and pyritic shale, siltstone, and coarse volcaniclastic sandstone with minor coal layers.|
16267|Rolling Downs Group|68901|6|Mentioned|p7 Fig. ii|||Eromanga Basin.|||Includes the Winton and Wallumbilla Formations.|||27-SEP-18
16267|Rolling Downs Group|69001|6|Mentioned|p2 Fig.1B, p30|Cretaceous|Cretaceous||||Includes the Doncaster Member.|||
16267|Rolling Downs Group|69297|6|Mentioned|p274 fig 4.3|Cenomanian|Early Cretaceous||||Includes the Wallumbilla Formation, Allaru Mudstone, Toolebuc Formation and the Normanton Formation.|||
16267|Rolling Downs Group|69455|6|Mentioned|p39:2, 39:4 Fig.39.3|Cretaceous|Cretaceous|Central Carpentaria Basin.||||||12-JUL-16
16267|Rolling Downs Group|69457|5|Briefly described|p41:2, 6, 8, 12|||Whitehouse (1955). Applies to the succession in SW Eromanga Basin, from the top of the (ungrouped) Cadna-owie Formation to the top of the Winton Formation. Up to c.1700m thick.|||Wilgunya, Manuka, Marree Subgroups.|Overlies Cadna-owie Formation.||12-JUL-16
16267|Rolling Downs Group|69555|6|Mentioned|p46||||||Includes Winton Formation|||
16267|Rolling Downs Group|69591|6|Mentioned|p29|Cretaceous|Jurassic|||||||
16267|Rolling Downs Group|69594|4|Described|p521-522, p540, p573-574|Late Cretaceous|Aptian|Carpentaria, Laura Basins. Source of lateritic bauxite (at Weipa) and kaolin, formed by deep weathering during the Late Cretaceous regression. The Group acts as the confining beds for the main aquifers in the Basin. Not subdivided in the Laura Basin, where it is up to 212m thick and is equivalent to the Wallumbilla Formation in the Eromanga Basin. Coeval with Allaru Mudstone. Youngest deposit in the Laura Basin.|||Wallumbilla, Toolebuc Formations; Allaru Mudstone; Normanton Formation.|Conformably overlies Gilbert River Formation. Is equivalent to upper Battle Camp Formation, Wolena Claystone.|Undivided: basal marine unit of calcareous and glauconitic shales with minor siltstone and conglomerate, overlain by silty and sandy marine claystones with carbonate concretions.|
16267|Rolling Downs Group|69599|5|Briefly described|p601-602|Cretaceous|Cretaceous|Lateritisation of this unit produced the world's largest bauxite deposit at Weipa.|||Normanton Formation.|||
16267|Rolling Downs Group|69673|6|Mentioned|p156||||||Includes Wilgunya Subgroup, Manuka Subgroup|||
16267|Rolling Downs Group|69682|5|Briefly described|p93 Fig.1|Cretaceous|Cretaceous|Eromanga and Surat Basins.||||||
16267|Rolling Downs Group|69952|5|Briefly described|p16|Cretaceous|Cretaceous|Eromanga Basin.|||Includes Winton and Wallumbilla Formations.|||
16267|Rolling Downs Group|69961|5|Briefly described|Map legend|Cretaceous|Cretaceous||||Includes Namur Sandstone?||Rounded, waterworn white vein quartz, quartzite, conglomerate, quartzose sandstones, siltstones and claystones; sparse marine fossils; large quartzite dropstones. Bioturbated marine white claystones, siltstones and fine-grained quartzose sandstones.|16-SEP-15
16267|Rolling Downs Group|70036|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Surat Basin. Included in a mapped unit of a marine sequence of semi-consolidated clay and claystone, minor fine quartz sandstone, coal and calcareous clay.||||||
16267|Rolling Downs Group|70207|6|Mentioned|p74|Cretaceous|Cretaceous|||||||
16267|Rolling Downs Group|70345|6|Mentioned|p3|Cretaceous|Cretaceous|||||||
16267|Rolling Downs Group|70352|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous||||Wilgunya Subgroup.|||
16267|Rolling Downs Group|70354|5|Briefly described|Map legend|Cretaceous|Cretaceous||||Wallumbilla, Toolebuc Formations; Allaru Mudstone.|||
16267|Rolling Downs Group|70572|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous||||Includes Wilgunya Subgroup.|||
16267|Rolling Downs Group|70648|5|Briefly described|Map Legend|Cretaceous|Cretaceous|2 un-named units: Marine white claystone, siltstone and fine-grained quartzose sandstone with bioturbation. Silicified variant.|||Includes 2 un-named units.||Rounded, waterworn, white vein quartz, quartzite, conglomerate, quartzose sandstone, siltstone and claystone; overall upward-fining sequence with sparse marine fossils and large, rounded quartzite dropstones.|
16267|Rolling Downs Group|70649|5|Briefly described|Map Legend|Cretaceous|Cretaceous||||Includes Winton Formation, Allaru Mudstone, Wallumbilla Formation.||Rounded, waterworn, white vein quartz, quartzite, conglomerate, quartzose sandstone, calcareous sandstone, siltstone and claystone; overall upward-fining sequence with sparse marine fossils and large, rounded quartzite dropstones.|
16267|Rolling Downs Group|70650|5|Briefly described|Map Legend|Cretaceous|Cretaceous||||||Rounded, waterworn, white vein quartz quartzite, conglomerate, quartzose sandstone, siltstone and claystone; overall upward-fining sequence with sparse marine fossils and large, rounded quartzite dropstones.|
16267|Rolling Downs Group|70651|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Includes unnamed sub-unit of marine white claystone, siltstone and fine-grained quartzose sandstone with bioturbation.|||Includes unnamed unit.||Rounded, waterworn, white vein quartz, quartzite, conglomerate, quartzose sandstone, siltstone and claystone; overall upward fining sequence with sparse marine fossils and large rounded quartzite dropstones.|
16267|Rolling Downs Group|70652|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Rounded quartz-rich gravel sourced from Namur Sandstone. Residual lag regolith and unconsolidated sediments also described.|||Includes Wallumbilla Formation.||Rounded, waterworn, white vein quartz, quartzite, conglomerate, quartzose sandstone, calcareous sandstone, siltstone and claystone; overall upward-fining sequence with sparse marine fossils and large, rounded quartzite dropstones.|
16267|Rolling Downs Group|70673|6|Mentioned|p7|Cretaceous|Cretaceous|||||||
16267|Rolling Downs Group|70821|5|Briefly described|p21, p30-31, p33, p80, p109, p113-114|Late Cretaceous|Early Cretaceous|Eromanga, Surat Basins; Coonamble Embayment. Formerly included Hooray Sandstone. Sediments locally occupy palaeovalleys (eg Gongolgon).|||Wallumbilla, Toolebuc, Mackunda, Griman Creek, Winton Formations; Surat Siltstone; Allaru Mudstone.|Overlies Bungil or Cadna-owie Formations and Drildool beds. Is overlain unconformably by Glendower Formation.||
16267|Rolling Downs Group|70836|6|Mentioned|p474|||Lightning Ridge area, Surat Basin.|||Griman Creek Formation.|||
16267|Rolling Downs Group|70860|6|Mentioned|p280-281|Cretaceous|Cretaceous|The main confining layer in the Great Artesian Basin.|||||A thick argillaceous marine sequence; mostly shallow-marine mudstone and siltstone.|
16267|Rolling Downs Group|71262|6|Mentioned|p9 Fig 7|Cretaceous|Cretaceous|||||||
16267|Rolling Downs Group|71342|6|Mentioned|Ch6 p12|||Originally subdivided by Whitehouse in 1926 who also subdivided this groups constituents into three sets of bed based on ammonite fauna. This scheme however was called into question by Casey (1960) and Day (1969). The validity of the Roma and Tambo Series was demonstrated by later workers (Dickins, 1960; Ludbrook, 1966; Day; 1969 and Morgan, 1980).|||Includes the Morven Bed, Roma Series, Maryborough Beds and the Tambo Series.|||
16267|Rolling Downs Group|71409|5|Briefly described|p1058-1059, p1061|Cretaceous|Cretaceous|Carpentaria Basin. Likely proximal source rocks for heavy minerals in central Cape York Peninsula. Outcrops in the northern tip of the Cape York Peninsula.||||Is overlain locally by Bulimba Formation.|Siltstones and claystones; deeply weathered and bauxitised.|23-APR-18
16267|Rolling Downs Group|71415|5|Briefly described|p11-p12|Late Cretaceous|Early Cretaceous|Geological province: SW Thomson Orogen. Of the Kooneberry Belt; of Eromanga Basin. Represents sedimentation from Early to Late Cretaceous before marine regression and closure of the Eromanga Basin (Exon and Senior 1976; Greenfield, Gilmore and Mills 2010).||||Uppermost unit of the Eromanga Basin. Underlain by Cadna-owie Formation.|Alternating sandstone, mudstone and calcareous units.|19-AUG-19
16267|Rolling Downs Group|71601|6|Mentioned|p121|||Geological province: Surat Basin.|||Includes Griman Creek Formation.|||
16267|Rolling Downs Group|71792|4|Described|p57-p58|Late Cretaceous|Early Cretaceous|Carpentaria Basin.|||||Grey mudstone, siltstone and fine sandstone, minor glauconitic sandstone.|
16267|Rolling Downs Group|71849|6|Mentioned|p8, p195|Cretaceous|Cretaceous|||||||
16267|Rolling Downs Group|71853|5|Briefly described|Map legend.|Late Cretaceous|Early Cretaceous|The two facies are mapped separately.|||||Siltstone and mudstone; minor glauconitic sandstone. Deeply weathered siltstone and mudstone; minor glauconitic sandstone.|
16267|Rolling Downs Group|71854|5|Briefly described|Map legend.|Late Cretaceous|Early Cretaceous||||||Siltstone and mudstone with minor glauconitic sandstone; Deeply weathered siltstone and mudstone with minor glauconitic sandstone.|08-MAY-19
16267|Rolling Downs Group|71855|6|Mentioned|p20, p30|||Structure is briefly discussed.|||Includes the Toolebuc Formation.|||
16267|Rolling Downs Group|71863|5|Briefly described|p4|Late Cretaceous|Middle Jurassic|Carpentaria Basin. Deposited during a marine incursion.|||Includes the Wallumbilla Formation, the Toolebuc Formation, Allaru Mudstone and Normanton Formation.|||01-MAY-19
16267|Rolling Downs Group|71864|6|Mentioned|p13|||First described by Isbell (1957).|||Includes the Wallumbilla Formation.|||
16267|Rolling Downs Group|71890|6|Mentioned|p7|||Surat Basin.|||Includes the Wallumbilla Formation.|||
16267|Rolling Downs Group|72298|5|Briefly described|p801|Cretaceous|Cretaceous|Eromanga Basin (SA,QLD,NSW), Carpentaria Basin, Surat Basin (QLD,NSW), Coonamble Embayment (NSW).|||Wallumbilla, Toolebuc, Mackunda, Winton, Normanton, Griman Creek FZs; Surat Siltstone; Allaru Mudstone.|Overlies Cadna-owie, Gilbert River, or Bungil FZ.||
16267|Rolling Downs Group|72914|6|Mentioned|p12|Cretaceous|Cretaceous|||||||
16267|Rolling Downs Group|72915|6|Mentioned|p12, p26|Mesozoic|Mesozoic|Sedimentary rocks in the Congararra 1 borehole are attributed to the Rolling Downs Group (map symbol suggests Cretaceous age), and may represent source-proximal Wallumbilla Formation (after Hawke and Cramsie, 1984). Represented in the Congararra 1 borehole by 41.15 m TVD thickness of interbedded claystone, siltstone, sandstone and arkose where the top portion is an indurated silcrete (to 23.53 m TVD), and is weathered to ~42 m TVD, before becoming fresh gravelly sand.|||||Interbedded claystone, siltstone, sandstone and arkose|
16267|Rolling Downs Group|72967|6|Mentioned|p5|||Carpenteria Basin.|||Allaru Mudstone, Toolebuc Formation, Wallumbilla Formation, Gilbert River Formation|||
16267|Rolling Downs Group|72983|6|Mentioned|p15|Cretaceous|Cretaceous|||||||
16267|Rolling Downs Group|73083|6|Mentioned|p51, p60-61, p68-69, p73|Mesozoic|Mesozoic|[Misspelt as Rolling Downs group on p61].|||Normanton Formation|||
16267|Rolling Downs Group|73144|6|Mentioned|p8|Cretaceous|Cretaceous|Carpentaria Basin. Contains units that constitute aquifers, partial aquifers, leaky aquitards and aquitards as well as host potential shale gas/oil plays and tight gas/oil.|||Normanton Formation, Allaru Mudstone, Toolebuc Formation, Wallumbilla Formation.|Underlain by Gilbert River Formation.||17-OCT-22
16267|Rolling Downs Group|73147|5|Briefly described|p128-129|Albian|Aptian|Marine.|||Wallumbilla, Toolebuc, Normanton Formations; Allaru Mudstone.|||
16267|Rolling Downs Group|73177|5|Briefly described|p1112|Late Jurassic|Late Jurassic|Relatively undeformed; gives a minimum age for the Alice Springs Orogeny.||||Unconformably overlies Ravendale Formation.||
16348|Roseneath Shale|13497|3|Fully described|iv, p69 fig 6.1, p70|Kungurian|Kungurian|Cooper Basin. Defined by Gatehouse (1972). Name derived from Roseneath Parish in Carruthers County, South West Queensland. Originally included as one of three units in the Moomba Formation before being raised to formation status by Gatehouse (1972). A type section is briefly mentioned. Maximum thickness of 100m. Petrography briefly discussed. A cross section where it contacts the Daralingie Formation is given on p99. This unit forms an important regional seal over the Epsilon Formation. Wireline log results are discussed. See also p93-p97, p99, p117, p129, p131, p160, p170-p175.||Gidgealpa Group||Intertongues with and conformably overlies the Epsilon Formation. Conformably overlain by the Daralingie Formation. Unconformably overlain by the Toolachee Foramtion.|Light to dark brown-grey or olive-grey siltstone, mudstone and minor sandstone. Siltstones are micromicaceous with minor fine-grained pyrite. Sandstone interbeds are pale brown and fine-grained.|
16348|Roseneath Shale|13516|6|Mentioned|p147, fig 5|Early Permian|Early Permian|From Cooper Basin||||||
16348|Roseneath Shale|22839|6|Mentioned|P33|||||||||
16348|Roseneath Shale|22883|6|Mentioned|P29|||||||||
16348|Roseneath Shale|23154|5|Briefly described|Map Legend|Early Permian|Early Permian|Geological Province - Cooper Basin.  Of the Gidgealpa Group.||||||17-JAN-08
16348|Roseneath Shale|23155|4|Described|p21|Early Permian|Early Permian|The Roseneath Shale is diachronous, younging southwest. The unit is up to 90m thick in the Mettika Embayment. Of Gidgealpa Group, Cooper Basin.||||||17-SEP-08
16348|Roseneath Shale|23340|6|Mentioned|12|||||||||
16348|Roseneath Shale|23375|4|Described|Fig2 p265,267,274,285||Kungurian|In the Cooper Basin.||||||17-JAN-08
16348|Roseneath Shale|23832|4|Described|p330|Permian|Permian|Of Gidgealpa Group. Geological Province: Cooper Basin.||||||
16348|Roseneath Shale|24210|5|Briefly described|p133 Fig. 2|Permian|Permian|Of the Gidgealpa Group.  Overlies the Epsilon Formation and Murteree Shale.  Geological Province: Cooper Basin.||||||
16348|Roseneath Shale|29387|6|Mentioned|Table 2|||Refers to Gatehouse(1972).||||||
16348|Roseneath Shale|29391|6|Mentioned|Table 5|||Appears on P23.||||||
16348|Roseneath Shale|29721|6|Mentioned|p161|||||||||
16348|Roseneath Shale|30540|6|Mentioned|Fig.6|||||||||
16348|Roseneath Shale|30544|6|Mentioned|p53|||Map legend||||||
16348|Roseneath Shale|30825|6|Mentioned|p37|||||||||
16348|Roseneath Shale|30873|2|Defined|p13|Permian|Permian|Part of Gidgealpa Group.||||||14-APR-08
16348|Roseneath Shale|30921|6|Mentioned|Map legend|Artinskian|Sakmarian|Sakmarian - Artinskian||||||
16348|Roseneath Shale|33074|6|Mentioned|p260|||||||||
16348|Roseneath Shale|33331|6|Mentioned|p39|||||||||
16348|Roseneath Shale|33489|6|Mentioned|Fig.2|||Refers Kapel (1972) & Gatehouse (1972)||||||
16348|Roseneath Shale|33976|6|Mentioned|Fig.5|||||||||
16348|Roseneath Shale|34839|6|Mentioned|Fig.2|||||||||
16348|Roseneath Shale|35067|6|Mentioned|Fig.4|||||||||
16348|Roseneath Shale|35068|6|Mentioned|Fig.3|||Discussed P60.||||||
16348|Roseneath Shale|35279|6|Mentioned|Fig.5|||||||||
16348|Roseneath Shale|35457|6|Mentioned|Fig.4|||Biostratigraphic relationships||||||
16348|Roseneath Shale|35573|6|Mentioned|Fig.7|||Generalised stratigraphy - Southern Cooper Basin||||||
16348|Roseneath Shale|35845|6|Mentioned|p24|||See also P73.||||||
16348|Roseneath Shale|36099|6|Mentioned|Fig.2|||||||||
16348|Roseneath Shale|36910|6|Mentioned|p62|||||||||
16348|Roseneath Shale|36917|6|Mentioned|Fig.1|||||||||
16348|Roseneath Shale|37855|6|Mentioned|Fig.2|||||||||
16348|Roseneath Shale|37917|6|Mentioned|Fig.2|||||||||
16348|Roseneath Shale|38977|6|Mentioned|p1422|||||||||
16348|Roseneath Shale|39252|5|Briefly described|p20|||||||||
16348|Roseneath Shale|39254|5|Briefly described|p46|||||||||
16348|Roseneath Shale|39261|6|Mentioned|Fig. 9|||||||||
16348|Roseneath Shale|39264|6|Mentioned|Fig. 13|||||||||
16348|Roseneath Shale|39276|6|Mentioned|Fig. 2|||||||||
16348|Roseneath Shale|39445|5|Briefly described|Table 8|||||||||
16348|Roseneath Shale|39478|6|Mentioned|Table 1|||||||||
16348|Roseneath Shale|39494|6|Mentioned|Fig.3|||||||||
16348|Roseneath Shale|40030|6|Mentioned|Fig.3|||||||||
16348|Roseneath Shale|40056|6|Mentioned|p11|||||||||
16348|Roseneath Shale|40249|6|Mentioned|p45|||||||||
16348|Roseneath Shale|40544|6|Mentioned|Fig.4|||||||||
16348|Roseneath Shale|41099|6|Mentioned|p190|||||||||
16348|Roseneath Shale|41131|5|Briefly described|Table 1|||||||||
16348|Roseneath Shale|41164|6|Mentioned|Fig.3|||||||||
16348|Roseneath Shale|41183|6|Mentioned|Fig.3 p308|||||||||
16348|Roseneath Shale|41189|6|Mentioned|Fig.4|||||||||
16348|Roseneath Shale|41198|6|Mentioned|Table 1|||||||||
16348|Roseneath Shale|41214|6|Mentioned|Fig.3|||||||||
16348|Roseneath Shale|41247|6|Mentioned|Fig.5|||||||||
16348|Roseneath Shale|41267|6|Mentioned|Fig.2|||||||||
16348|Roseneath Shale|41288|6|Mentioned|p159|||||||||
16348|Roseneath Shale|41595|6|Mentioned|p42|||||||||
16348|Roseneath Shale|41707|6|Mentioned|Fig.8|||||||||
16348|Roseneath Shale|41720|6|Mentioned|p373|||||||||
16348|Roseneath Shale|42085|6|Mentioned|Fig.2 P374|||||||||
16348|Roseneath Shale|42746|5|Briefly described|p6|||||||||
16348|Roseneath Shale|42999|5|Briefly described|Table 2,p90||Early Permian|||||||
16348|Roseneath Shale|43002|5|Briefly described|Fig.2,p135|||||||||
16348|Roseneath Shale|43018|5|Briefly described|Table 1,p386|||||||||
16348|Roseneath Shale|43105|5|Briefly described|Fig.7,p13|||||||||
16348|Roseneath Shale|43570|5|Briefly described|Fig.2,p535,544,545||Kungurian|||||||
16348|Roseneath Shale|44133|5|Briefly described|p65 Fig. 8.3, 85|Kungurian|Kungurian|Of the Gidgealpa Group. Geological Province: Cooper Basin. Overlies: Epsilon Formation. Underlies: Daralingie Formation.||||||
16348|Roseneath Shale|46849|6|Mentioned|Fig. 7|||||||||
16348|Roseneath Shale|60386|6|Mentioned|p296|Kungurian|Kungurian|Cooper Basin. Non-marine.||||||
16348|Roseneath Shale|60717|5|Briefly described|p40 Fig. 2|Kungurian|Kungurian|Of Gidgealpa Group. Overlies Epsilon Formation; underlies Daralingie Formation. Geological province: Cooper Basin.||||||
16348|Roseneath Shale|61615|5|Briefly described|p302, p302 Fig. 2, p304|Early Permian|Early Permian|Of Gidgealpa Group. Underlain by Epsilon Formation. Geological Province: Cooper Basin.||||||30-APR-13
16348|Roseneath Shale|61616|6|Mentioned|p330 Fig. 2|Early Permian|Early Permian|Of Gidgealpa Group. Geological Province: Cooper Basin.||||||31-MAR-09
16348|Roseneath Shale|62046|5|Briefly described|p125 Fig. 2|Permian|Permian|Geological Province: Cooper-Eromanga Basins.||||||14-APR-08
16348|Roseneath Shale|62537|6|Mentioned|p191 Fig.2. |Early Permian|Early Permian|Cooper Basin.||Unit in Gidgealpa Group.||Overlies Epsilon Formation. Is overlain by Daralingie Formation.||
16348|Roseneath Shale|63832|6|Mentioned|p131 fig 2|Kungurian|Kungurian|Cooper Basin.||||||
16348|Roseneath Shale|63978|2|Defined|p15, Fig. 3|Middle Permian|Early Permian|Conformable over/intertongues with Epsilon Fm; overlain/intertongues with Daralingie Fm; unconformable below Toolachee Fm.in places. Max. thick: 99m. Laminated siltstone, mudstone and lesser sandstone (carbonaceous). more lith.included. In Cooper Basin.||||||07-FEB-11
16348|Roseneath Shale|64048|5|Briefly described|p63, p64 Tb. 2|||Geological Province: Cooper Basin. Acts as the seal for Epsilon Formation reservoirs.||||||07-FEB-11
16348|Roseneath Shale|64197|6|Mentioned|p625 Fig.1c, p630 Fig.7|Permian|Permian|Cooper Basin.||||Underlies Daralingie [Beds] Formation, overlies Epsilon and Patchawarra Formations.||11-DEC-15
16348|Roseneath Shale|64665|5|Briefly described|p53 Fig.2.|Middle Permian|Middle Permian|Cooper Basin.||||Overlies Epsilon Formation. Is overlain by Daralingie Formation.||
16348|Roseneath Shale|65489|5|Briefly described|p45, p48-49, p96, p131-132, p143|Kungurian|Kungurian|Cooper Basin. Relatively little hydrocarbon source potential. Regional seal of the Epsilon Formation.||Unit in Gidgealpa Group.||Overlies Epsilon Formation and Murteree Shale. Is overlain by Daralingie Formation.|Lacustrine shale unit.|
16348|Roseneath Shale|65925|5|Briefly described|Appendix 2.||||||||Siltstone, shaly, with minor sandstone lenses. Lacustrine, diachronous.|
16348|Roseneath Shale|67402|5|Briefly described|p90, p90 fig CPR4|||Cooper Basin. 50-100m thick. Distal lacustrine deposits. Forms regionally extensive seal to the Epsilon Formation. See also p91 tbl CPR1, p92, p93, p96, p98, p101 tbl CPR2.||Gidgealpa Group||Overlies the Epsilon Formation. Overlain by the Daralingie Formation.|Laminated carbonaceous siltstone, mudstone and minor thin beds of fine-grained sandstone.|
16348|Roseneath Shale|68731|5|Briefly described|p200 Fig 3.110, p204, p205, p206|Guadalupian||Gatehouse (1972). Along with the Murteree Shale and Epsilon Formation, the Roseneath Shale replaces the Moomba Formation. ~ 20-100 m thick. Palynofloral assemblages suggest latest Kungurian(?)-early Wordian (Price 1997).||Of the Gidgealpa Group.||Conformably underlain by the Epsilon Formation. Conformably/unconformably overlain by the Daralingie and Toolachee Formations respectively. Intertongues with the Epsilon and Daralingie Formations.|Includes laminated, carbonaceous, micro-micaceous siltstones with pyrite and siderite, and mudstone and lesser fine sandstone, the latter forming beds rarely > 2 m thick.|18-JUL-14
16348|Roseneath Shale|69023|5|Briefly described|p81, p82 Fig.18, p85|Permian|Permian|Cooper Basin. Lacustrine.||Unit in Gidgealpa Group.||||
16348|Roseneath Shale|69454|5|Briefly described|p38:4|Wordian|Kungurian|Cooper Basin.||Gidgealpa Group.||||12-JUL-16
16348|Roseneath Shale|69673|6|Mentioned|p153 fig 125|||||Gidgealpa Group||Overlain by Daralingie Formation, overlies Epsilon Formation||
16348|Roseneath Shale|69797|5|Briefly described|p17 Fig.2|Early Permian|Early Permian|Age: Kungarian (approximated from figure). Geol. Prov: Cooper Basin.||Gidgealpa Group||||
16348|Roseneath Shale|69946|5|Briefly described|p9, p36, p45, p54|Kungurian|Kungurian|Cooper Basin. Lacustrine.||Unit in Gidgealpa Group.||Overlies Epsilon and Patchawarra Formations. Is overlain by Daralingie Formation.||
16348|Roseneath Shale|69947|5|Briefly described|p13 Fig.7.2|Permian|Permian|Cooper Basin.||Gidgealpa Group.||||
16348|Roseneath Shale|70317|6|Mentioned|p33-34, 36|Early Permian|Early Permian|Cooper Basin. Vertical section showing fracture densities.||Gidgealpa Group.||Overlies Epsilon Formation. Is overlain by Daralingie Formation.||
16348|Roseneath Shale|70823|4|Described|iv, p1, p3, p6|Wordian|Roadian|Cooper Basin. Hosts shale gas plays. Seismic reflection, palynological and outcrop characteristics briefly discussed. On the basis of spore pollen zones this unit has been dated at 269.6 Ma and 266.8 Ma. Up to 240m thick. Deposited in a lacustrine environment. Contains potential source rock facies. See also p14-p15, p25-p27, p38, p40-p41, p54, p59, p64-p65, p78, p82-p83.||Gidgealpa Group||Intertongues with and conformably overlies the Epsilon Formation. Conformably overlain by the Daralingie Formation.|Light to dark brown-grey siltstone, mudstone and minor fine-grained sandstone units.|
16348|Roseneath Shale|70824|4|Described|p1, p3, p7-p9, p30-p31|Wordian|Roadian|Cooper Basin. Hosts shale gas plays. Deposited in a lacustrine environment. Up to 240m thick. Forms a hydrocarbon seal over the Epsilon Formation. Outcrop, areal extent and source rock geochemistry are discussed. See also p77-p83, p108-p109, p113, p123.||||Overlies the Epsilon Formation. Overlain by the Daralingie Formation.|Light to dark brown-grey siltstone, mudstone and minor fine-grained sandstone units.|
16348|Roseneath Shale|70946|5|Briefly described|p1087, p1089-1091, p1096|Permian|Early Permian|Cooper Basin. Hosts shale gas plays. Up to 194m thick. HyLogging was combined with XRD and core petrology to target fracture stimulation. Deposited in lacustrine with interbedded fluvio-deltaic transgressive/regressive shoreface environments.||Gidgealpa Group.||Overlies Epsilon Formation. Is overlain by Daralingie Formation.|Siltstones, siliceous (and sideritic in part) mudstones.|08-OCT-18
16348|Roseneath Shale|71059|6|Mentioned|p6 Fig.5|||Cooper Basin.||||||
16348|Roseneath Shale|71265|5|Briefly described|p589|Wordian|Roadian|Cooper Basin.||Gidgealpa Group.||Overlies Epsilon Formation. Is overlain by Daralingie Formation.||
16348|Roseneath Shale|71342|5|Briefly described|Ch5 p3, Ch5 p9|Kazanian|Kungurian|Cooper Basin. Deposited in a lacustrine environment.  Palynological zone is given in fig 5.3 Ch5 p36. See also Ch5 p36, Ch5 p45, Ch5 p54, Ch7 p13.||Gidgealpa Group||||
16348|Roseneath Shale|71701|5|Briefly described|p155|Wordian|Roadian|Cooper Basin.||Gidgealpa Group||Overlies the Epsilon Formation. Overlain by the Daralingie Formation.||
16348|Roseneath Shale|71863|6|Mentioned|p2|Paleozoic|Paleozoic|Cooper Basin.||||||
16348|Roseneath Shale|72297|6|Mentioned|p742|||Cooper Basin. Acts as a regional seal.||||||
16348|Roseneath Shale|73167|6|Mentioned|p662, p664|late Permian|late Permian|Cooper Basin. Deposited in an east-to-west late Permian transgression of fluvio-deltaic, shoreface and lacustrine sediments.||||||
16348|Roseneath Shale|73244|6|Mentioned|p86|Permian|Permian|Cooper Basin. Fluvio-deltaic/lacustrine environment.||||||
16348|Roseneath Shale|73251|6|Mentioned|p62|Cisuralian|Cisuralian|Cooper Basin. Lacustrine depositional environment. Hydrocarbon source rock.||Gidgealpa Group||Underlain by Epsilon Formation. Overlain by Daralingie Formation.||
16348|Roseneath Shale|73343|6|Mentioned|p337-338|Late Permian|Late Permian|Cooper Basin.||||Underlain by Murteree Shale. Unconformably overlain by Toolachee Formation. Equivalent to Daralingie Formation.||
16348|Roseneath Shale|73479|5|Briefly described|p156 Fig.2, p159, p163|Permian|Permian|Cooper Basin. Fluvio-deltaic/lacustrine depositional environment. Highly efficient regional seal.|ca 260 Ma|||Unconformably underlies Toolachee Formation||
16348|Roseneath Shale|73495|6|Mentioned|p497, p499-500|Captainian|Wordian|Cooper Basin. Part of the REM succession.||||Underlain by Epsilon Formation. Overlain by Daralingie Formation.||
16445|Rumbalara Shale|22566|5|Briefly described|p79|Mesozoic|Mesozoic|Of the Finke Group.||||||28-NOV-06
16445|Rumbalara Shale|22826|6|Mentioned|p576|Early Cretaceous|Early Cretaceous|Geological Province - Eromanga Basin.||||||
16445|Rumbalara Shale|23818|6|Mentioned|p141 Fig.65|||Geological Province: Great Artesian Basin.||||||
16445|Rumbalara Shale|33165|6|Mentioned|Chart|||Correlation chart only||||||
16445|Rumbalara Shale|33832|5|Briefly described|p11|||Correlation and strat.||||||28-NOV-06
16445|Rumbalara Shale|33844|6|Mentioned|Table 1|||||||||
16445|Rumbalara Shale|33939|6|Mentioned|p412|||Lithology.  L.Cret.||||||
16445|Rumbalara Shale|33971|5|Briefly described|p26|||||||||
16445|Rumbalara Shale|34111|5|Briefly described|Table 3|||Cretaceous. See also pp16,18,19.||||||28-NOV-06
16445|Rumbalara Shale|34580|4|Described|Table 1|||Lower Cretaceous||||||
16445|Rumbalara Shale|34611|6|Mentioned|Fig.65|||Correlation chart.||||||
16445|Rumbalara Shale|34971|6|Mentioned|p296|||||||||
16445|Rumbalara Shale|36751|6|Mentioned|p490|||||||||
16445|Rumbalara Shale|40926|6|Mentioned|p17|||||||||
16445|Rumbalara Shale|42504|5|Briefly described|p83|||||||||
16445|Rumbalara Shale|42940|6|Mentioned|p2|||||||||
16445|Rumbalara Shale|43035|6|Mentioned|p26|||||||||
16445|Rumbalara Shale|44222|14|Not recorded|p107|||||||||
16445|Rumbalara Shale|44323|14|Not recorded|map legend||Early Cretaceous|SG/53-6. L.Cretaceous.||||||
16445|Rumbalara Shale|44335|4|Described|p.13||Cretaceous|Tb.3. p.14. L.Cretaceous.||||||
16445|Rumbalara Shale|44336|14|Not recorded|map legend||Early Cretaceous|SG/53-3. L.Cretaceous.||||||
16445|Rumbalara Shale|44342|5|Briefly described|p.8 Table 8||Early Cretaceous|SG/53-5.. L.Cretaceous.||||||
16445|Rumbalara Shale|44343|14|Not recorded|map legend||Early Cretaceous|L.Cretaceous.||||||
16445|Rumbalara Shale|44393|4|Described|p.6,7,10,Tb.1,Fig.1||Aptian|||||||
16445|Rumbalara Shale|44394|14|Not recorded|map legend||Early Cretaceous|Lower Cretaceous.||||||
16445|Rumbalara Shale|44433|14|Not recorded|map legend||Cretaceous|||||||
16445|Rumbalara Shale|44946|14|Not recorded|Not recorded|||||||||
16445|Rumbalara Shale|45011|4|Described|p9-13,15|||Same age as Roma and Lower Wilgunya Formations.||||||
16445|Rumbalara Shale|45041|4|Described|p114|||L. Cret.||||||
16445|Rumbalara Shale|46740|14|Not recorded|p.187||Cretaceous|||||||
16445|Rumbalara Shale|48639|14|Not recorded|opp.p.1,map||Cretaceous|Cret.||||||
16445|Rumbalara Shale|48865|2|Defined|p.39||Early Cretaceous|Many figures. Fig.4,37,38,41,Fig.13,51,53,Pl.6,10,11. Lower Cretaceous. (G53-3,6).||||||
16445|Rumbalara Shale|48880|14|Not recorded|p.17,20,Pl.13||Early Cretaceous|L.Cret.(G53-3).||||||
16445|Rumbalara Shale|48890|2|Defined|p.56||Early Carboniferous|See also Tb.2,3,Fig.4,p.26,27. Pl.10. Lower Carboniferous.||||||
16445|Rumbalara Shale|48963|6|Mentioned|Plate 5|||||||||
16445|Rumbalara Shale|50372|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Geological Province: Eromanga Basin. Very fine grained siltstone, commonly silicified to porcellanite.||||||
16445|Rumbalara Shale|61155|5|Briefly described|p16|||Age is pre-Cainozoic. Geological Province: East Amadeus Basin.||||||
16445|Rumbalara Shale|62609|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Siltstone, porcellanite, some sandstone. Overlies: De Souza Sandstone.||||||14-AUG-06
16445|Rumbalara Shale|62620|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Siltstone, porcellanite, some sandstone.||||||
16445|Rumbalara Shale|65309|6|Mentioned|p14.|||Probable correlative of Bulldog Shale in South Australia.||||Overlies Algebuckina Sandstone.||
16445|Rumbalara Shale|65342|6|Mentioned|p10.|||Pedirka Basin. Max. thickness at least 407 m.  Seen as having potential as an insulating layer for geothermal energy.||||Overlies Cadna-owie Formation.||
16445|Rumbalara Shale|68734|6|Mentioned|p221 Fig.3|Cretaceous|Cretaceous|||||||
16445|Rumbalara Shale|69457|5|Briefly described|p41:3-4, 8, 10, 14-15|Early Cretaceous|Early Cretaceous|Wells (1969). Described as a "local" name in the western Eromanga Basin (NT) for fine-grained exposures at a similar stratigraphic level that, in the FINKE map area, were later assigned to the Bulldog Shale? by Edgoose et al. (2002). They are here referred to as unassigned Wilgunya Subgroup, or as Bulldog Shale/Wallumbilla Formation, and the unit's name appears to be obsolete. c.275m thick. Hosts the Rumbalara Ochre Mine, mined between 1939 and 1951 for paint pigment.||||Disconformably/unconformably overlay De Souza Sandstone.||12-JUL-16
16445|Rumbalara Shale|69458|6|Mentioned|p42:16|||Eromanga Basin. Some rocks of the Wilgunya Subgroup in HALE RIVER, McDILLS map areas are mapped under this name.||||||12-JUL-16
16445|Rumbalara Shale|71321|6|Mentioned|p27|||||||Equivalent to Bulldog Shale.||
16445|Rumbalara Shale|72298|5|Briefly described|p801|Cretaceous|Cretaceous|Eromanga Basin (NT).||||Overlies DeSouza Sandstone. Is overlain by Winton FZ.||
16445|Rumbalara Shale|73281|6|Mentioned|Appendix (DIP)|||See DIP034_Petroleumdata.xlsx and DIP034_Welldata.xlsx.||||||
16454|Runnymede Formation|24551|6|Mentioned|p247|||At Killara Bluff in the Casterton area. Name proposed to be abandoned by Duddy (1983). Equivalent to Eumeralla Formation.||||||12-JAN-10
16454|Runnymede Formation|31245|6|Mentioned|p79|||L. Cretaceous||||||
16454|Runnymede Formation|31625|6|Mentioned|Fig. 5.2|||L.Cret.||||||
16454|Runnymede Formation|31920|5|Briefly described|p49|||Unit of Merino Gp.||||||
16454|Runnymede Formation|34148|6|Mentioned|p272|||||||||
16454|Runnymede Formation|41642|6|Mentioned|p218|||||||||
16454|Runnymede Formation|42827|5|Briefly described|Table 7.2|||of Otway Group||||||
16454|Runnymede Formation|48624|14|Not recorded|p5|||(J54-6/Benara).||||||
16454|Runnymede Formation|48625|14|Not recorded|p5|||(J54-6/Kennion).||||||
16454|Runnymede Formation|48911|6|Mentioned|Chart 1|||||||||
16461|Russo beds|42723|5|Briefly described|map legend|Pleistocene||Variation on Russo Beds.||||||
16480|Ruwarung Member|22525|6|Mentioned|p37||Eocene|Superseded by Port Willunga Formation.||||||12-NOV-08
16480|Ruwarung Member|22528|6|Mentioned|p43 Fig2||Oligocene|||||||
16480|Ruwarung Member|22541|4|Described|p 30, Table 1||Early Oligocene|Port Willunga Formation.||||||12-NOV-08
16480|Ruwarung Member|22587|6|Mentioned|p79 Fig.7|Early Oligocene|Early Oligocene|||||||
16480|Ruwarung Member|23418|6|Mentioned|p14 Fig.4|||||||||
16480|Ruwarung Member|30250|2|Defined|p2|Eocene|Eocene|||||||
16480|Ruwarung Member|35689|2|Defined|p23|Oligocene|Oligocene|||||||
16480|Ruwarung Member|36127|5|Briefly described|p11|||See also P7.||||||
16480|Ruwarung Member|36244|6|Mentioned|p2|||Defined by Cooper 1977, 1979.||||||
16480|Ruwarung Member|36500|6|Mentioned|Fig.4|||||||||
16480|Ruwarung Member|37324|6|Mentioned|p11|||||||||
16480|Ruwarung Member|38107|4|Described|p37|||||||||
16480|Ruwarung Member|38702|6|Mentioned|p127|||||||||
16480|Ruwarung Member|39351|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
16480|Ruwarung Member|40238|6|Mentioned|Fig.1|||||||||
16480|Ruwarung Member|40429|6|Mentioned|Fig.2|||||||||
16480|Ruwarung Member|40453|5|Briefly described|p57|||||||||
16480|Ruwarung Member|40877|5|Briefly described|p50|||||||||
16480|Ruwarung Member|40970|6|Mentioned|p16|||||||||
16480|Ruwarung Member|41025|5|Briefly described|p172|||||||||
16480|Ruwarung Member|41495|6|Mentioned|Table 5|||||||||
16480|Ruwarung Member|41513|6|Mentioned|p42|||||||||
16480|Ruwarung Member|41517|6|Mentioned|p138|||See also P139||||||
16480|Ruwarung Member|41520|5|Briefly described|Fig.5|||||||||
16480|Ruwarung Member|42498|5|Briefly described|Map Legend|Oligocene|Oligocene|||||||
16480|Ruwarung Member|44133|5|Briefly described|p165 Fig. 10.11, 168|Late Oligocene|Early Oligocene|Geological Province: Saint Vincent Basin. Of the Port Willunga Formation.||||||
16480|Ruwarung Member|60538|5|Briefly described|p479 Fig. 18|Oligocene|Eocene|Geological Province: Saint Vincent Basin. Of the Port Willunga Formation.||||||
16480|Ruwarung Member|60785|5|Briefly described|p184 Fig.1, p194.  |Rupelian|Rupelian|South Australia. Willungan age (Early Oligocene; Rupelian) 30-32 Ma (Alley et al., 1995; Holdgate and Gallagher, 2003). Has yielded fossil cetacean elements.||Of the Port Willunga Formation.|||Bryozoal marl limestone, containing chert nodules.|
16480|Ruwarung Member|61155|5|Briefly described|p17|Early Oligocene|Early Oligocene|See also Ruwarung member. Of the Port Willunga Formation. Overlies and interfingers with Aldinga Member; laterally interfingers with Pirramimma Sand Member. Age: 36-30Ma. Geological Province: St Vincent Basin.||||||
16480|Ruwarung Member|64397|5|Briefly described|p232 Fig. 1A, p233|Oilgocene|Oilgocene|Upper part of Port Willunga Formation. Succession of mostly limestone and marl with conspicuous chert nodules and layers. Detailed lithological chart presented - p237, Fig. 5. See also p245 Fig. 11. Geological province: St Vincent Basin.||||||
16480|Ruwarung Member|64993|5|Briefly described|p2p Fig. 5|||Of Port Willunga Formation. Geological province: St Vincent Basin. Siliceous calcarenite with cherty concretions. Contains a cypraeid bed (molluscan assemblages).||||||
16480|Ruwarung Member|65375|4|Described|p36.|||To 15m thick. Limestone is dominantly bryozoan; voids filled with sparry cement or calcareous sand or silt. Overlain by 3m thick un-named member of massive, silty to sandy limestone. Correlated with Rogue Formation.||Middle unit in Port Willunga Formation.||Overlies Aldinga Member.|Pink-brown, massive to thick-bedded skeletal limestone; minor marl or silty limestone.|
16480|Ruwarung Member|65891|5|Briefly described|p221 Fig.5, p222 Fig.7. |Paleogene|Paleogene|Unit in upper Port Willunga Formation. Overlies Aldinga Member. Rupelian age.||||||
16480|Ruwarung Member|66131|6|Mentioned|p242 Fig.2|Oligocene|Eocene|Late Eocene to late Oligocene in age (from p.242 Fig.2 - stratigraphic correlation chart).||Unit in Port Willunga Formation.||Overlies Aldinga Member.||
16480|Ruwarung Member|67462|5|Briefly described|Map legend.||Oligocene|Eastern Saint Vincent Basin.||Unit in Port Willunga Formation.||||
16480|Ruwarung Member|68715|6|Mentioned|p31 Fig.5|Rupelian|Rupelian|St Vincent Basin.||||||
16480|Ruwarung Member|70660|5|Briefly described|p8-p9, p12, p20, p22, p25, p32, p46|Rupelian|Rupelian|||Port Willunga Formation||Overlies the Aldinga Member. Overlain by the Janjukian Unit.|Soft, silty and clayey limestone with fossiliferous cherts.|
16480|Ruwarung Member|70722|5|Briefly described|p217-218|Late Oligocene|Early Oligocene|Of St. Vincent Basin. Equivalent to Kingscote Limestone Unit K4 of this study.||Unit of Port Willunga Formation.||Overlain by Janjukian Unit. Underlain by Aldinga Member.||
16480|Ruwarung Member|73107|5|Briefly described|Map legend.|||St. Vincent Basin. Equivalent to an un-named Oligocene unit of silicified dolomitic calcilutite, boulders of which are washed up at Cape Hart, Point Reynolds, Cape Linois and Cape Gantheaume.||||||
16480|Ruwarung Member|73188|6|Mentioned|p320|Oligocene|Oligocene|St Vincent Basin.||Port Willunga Formation|||Limestone, marl, clay.|
16502|Saddleworth Formation|22631|6|Mentioned|p177|Cryogenian|Cryogenian|||||||
16502|Saddleworth Formation|22889|4|Described|p35|Adelaidean|Adelaidean|Of the Bungarider Subgroup. New Members are included in the Saddleworth Formation, see p35 for details.||||||14-MAY-07
16502|Saddleworth Formation|22926|6|Mentioned|43|||Parent Burra Group.||||||27-MAY-08
16502|Saddleworth Formation|23482|5|Briefly described|p10|Adelaidean|Adelaidean|||||||
16502|Saddleworth Formation|23731|6|Mentioned|p29|Adelaidean|Adelaidean|||||||
16502|Saddleworth Formation|23818|4|Described|p60|Neoproterozoic|Neoproterozoic|Max. thickness: 4500 ft. (Thickness varies, as Auburn Dolomite becomes the Saddleworth Formation). Underlain by Auburn Dolomite.||||||14-MAY-07
16502|Saddleworth Formation|23869|5|Briefly described|p20|||||||||
16502|Saddleworth Formation|24546|5|Briefly described|p2 - 3 Fig.2|Neoproterozoic|Neoproterozoic|Of Burra Group. Geological Province: Adelaide Fold Belt.||||||16-JAN-08
16502|Saddleworth Formation|29780|4|Described|p28|||||||||
16502|Saddleworth Formation|30051|6|Mentioned|p12|||||||||
16502|Saddleworth Formation|30052|6|Mentioned|Fig.5|||||||||
16502|Saddleworth Formation|30090|6|Mentioned|p4|||||||||
16502|Saddleworth Formation|30782|6|Mentioned|p70|||Refers stratigraphy||||||
16502|Saddleworth Formation|30801|6|Mentioned|p5|||Table P5-6||||||
16502|Saddleworth Formation|30807|6|Mentioned|p103|||Suggested map symbol||||||
16502|Saddleworth Formation|31292|6|Mentioned|p5|||Refers Wilson (1952)||||||
16502|Saddleworth Formation|31923|6|Mentioned|p9|||||||||
16502|Saddleworth Formation|32031|6|Mentioned|p168|||Fig.1||||||
16502|Saddleworth Formation|32510|6|Mentioned|Table 1|||||||||
16502|Saddleworth Formation|32547|6|Mentioned|Fig.2|||Torrensian||||||
16502|Saddleworth Formation|32720|6|Mentioned|Table 1|||||||||
16502|Saddleworth Formation|32722|6|Mentioned|Fig.3|||Adelaidean. Stromatolite||||||
16502|Saddleworth Formation|32724|6|Mentioned|Fig.1|||Torrensian. Correlation||||||
16502|Saddleworth Formation|33422|6|Mentioned|Map legend|Precambrian|Precambrian|||||||
16502|Saddleworth Formation|33423|4|Described|p13|||||||||
16502|Saddleworth Formation|33474|6|Mentioned|Fig.2|||||||||
16502|Saddleworth Formation|33577|6|Mentioned|p80|||Geol. map. Shale deposits P79||||||
16502|Saddleworth Formation|33956|4|Described|p1040|||||||||
16502|Saddleworth Formation|34308|6|Mentioned|p189|||||||||
16502|Saddleworth Formation|34320|6|Mentioned|Fig.|||Regional geology plan.||||||
16502|Saddleworth Formation|34521|5|Briefly described|p156|||Equivalent unit. Suitability for road-making||||||
16502|Saddleworth Formation|34535|5|Briefly described|p60|||See Fig.19||||||
16502|Saddleworth Formation|34536|6|Mentioned|Map legend|Adelaidean|Adelaidean|Torrensian||||||
16502|Saddleworth Formation|34587|5|Briefly described|p36|||||||||
16502|Saddleworth Formation|35090|6|Mentioned|Fig.1|||||||||
16502|Saddleworth Formation|35200|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
16502|Saddleworth Formation|35232|6|Mentioned|p5|||See also Table.1||||||
16502|Saddleworth Formation|36126|6|Mentioned|Fig.1|||||||||
16502|Saddleworth Formation|36623|6|Mentioned|Fig.1|||||||||
16502|Saddleworth Formation|36625|6|Mentioned|Fig.1|||||||||
16502|Saddleworth Formation|36733|6|Mentioned|Table 5|||||||||
16502|Saddleworth Formation|36835|6|Mentioned|p31|||||||||
16502|Saddleworth Formation|37461|6|Mentioned|Table 5.I|||||||||
16502|Saddleworth Formation|38157|6|Mentioned|Table III|||||||||
16502|Saddleworth Formation|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Torrensian||||||
16502|Saddleworth Formation|39350|6|Mentioned|Map legend|Adelaidean|Adelaidean|Torrensian||||||
16502|Saddleworth Formation|39351|6|Mentioned|Map legend|Adelaidean|Adelaidean|Torrensian||||||
16502|Saddleworth Formation|40442|6|Mentioned|Fig.4|||||||||
16502|Saddleworth Formation|40456|6|Mentioned|Fig.2|||||||||
16502|Saddleworth Formation|40500|5|Briefly described|Fig.2|||||||||
16502|Saddleworth Formation|40501|6|Mentioned|p115|||||||||
16502|Saddleworth Formation|40852|6|Mentioned|Fig.3.2|||||||||
16502|Saddleworth Formation|41404|3|Fully described|p110|||Type section described.||||||24-SEP-15
16502|Saddleworth Formation|41405|6|Mentioned|Fig.50|||||||||
16502|Saddleworth Formation|41494|6|Mentioned|p30|||||||||
16502|Saddleworth Formation|41526|6|Mentioned|p8|||||||||
16502|Saddleworth Formation|42093|6|Mentioned|p9|||See also Fig.7||||||
16502|Saddleworth Formation|42098|5|Briefly described|p53|||||||||
16502|Saddleworth Formation|42104|6|Mentioned|p90|||||||||
16502|Saddleworth Formation|42222|5|Briefly described|p14|||||||||
16502|Saddleworth Formation|42243|5|Briefly described|p211|||||||||
16502|Saddleworth Formation|42505|5|Briefly described|Map legend|Adelaidean (Torrensian)|Adelaidean (Torrensian)|||||||
16502|Saddleworth Formation|42506|5|Briefly described|Map legend|Adelaidean (Torrensian)||||||||
16502|Saddleworth Formation|42574|5|Briefly described|p241|||||||||
16502|Saddleworth Formation|42720|5|Briefly described|map legend|Torrensian||||||||
16502|Saddleworth Formation|42733|6|Mentioned|map legend|Adelaidean||||||||
16502|Saddleworth Formation|42761|5|Briefly described|Fig.2 P8|||Of the Burra Group.||||||14-MAY-07
16502|Saddleworth Formation|42813|5|Briefly described|p16|||Of the Burra Group.||||||14-MAY-07
16502|Saddleworth Formation|43052|5|Briefly described|p181,Table 6.1|||Of the Burra Group.||||||14-MAY-07
16502|Saddleworth Formation|43742|6|Mentioned|p43|||||||||
16502|Saddleworth Formation|44133|6|Mentioned|p46, 207|Precambrian|Precambrian|||||||
16502|Saddleworth Formation|44690|4|Described|map legend|||Geol. Atlas Series. (I/54-5). Torrensian.||||||
16502|Saddleworth Formation|48894|6|Mentioned|p70|||Age||||||
16502|Saddleworth Formation|50615|5|Briefly described|p303 Fig. 2, p304 Fig. 4|||Geological Province: Adelaide Fold Belt. See also p304 Fig. 3.||||||
16502|Saddleworth Formation|60959|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Of the Burra Group. Dolomitic siltstone, fine grained sandstone, dark grey dolomite.||||||
16502|Saddleworth Formation|61238|4|Described|p46 Fig. 2, p47 Fig. 3|Neoproterozoic|Neoproterozoic|Of the Burra Group. Mudstone; siltstone; shale; partly carbonaceous.||||||
16502|Saddleworth Formation|61307|5|Briefly described|p25 Fig. 14|Torrensian|Torrensian|Of the Burra Group. Geological Province: Adelaide Fold Belt.||||||
16502|Saddleworth Formation|62724|5|Briefly described|p17 Fig. 4|Torrensian|Torrensian|Of the Bungarider Subgroup (Burra Group).||||||07-FEB-11
16502|Saddleworth Formation|64647|5|Briefly described|p39 Fig. 2, p40|Neoproterozoic|Neoproterozoic|Of Burra Group. Phyllite, dolomitic phyllite, dolomite, quartzite.||||||
16502|Saddleworth Formation|64796|6|Mentioned|p191 Fig.9|Neoproterozoic|Neoproterozoic|||||Overlies Auburn Dolomite. Is overlain by Mintaro Shale.||
16502|Saddleworth Formation|65925|5|Briefly described|Appendix 2.||||||||Mudstone; siltstone; shale, partly carbonaceous.|
16502|Saddleworth Formation|66522|5|Briefly described|p23.|Neoproterozoic|Neoproterozoic|||Unit in Bungarider Subgroup.|||Laminated siltstone with variable carbonate content and lenticular thin sandy interbeds.|
16502|Saddleworth Formation|70405|6|Mentioned|p51 table 4|Neoproterozoic|Neoproterozoic|||Bungarider Subgroup|Includes Watervale Sandstone Member|||
16502|Saddleworth Formation|70819|5|Briefly described|p11, 13-16, 24-25, 28|Neoproterozoic|Neoproterozoic|Clare Valley.|c.750 Ma.|Bungarider Subgroup.||Overlies Watervale Sandstone. Is overlain by Leasingham Quartzite.|Deeper shelf silty sediments; grey, dolomitic siltstone.|
16502|Saddleworth Formation|71237|14|Not recorded|p9, 18|||||||||
16502|Saddleworth Formation|71240|14|Not recorded|p7, p9, p18|||||||||
16502|Saddleworth Formation|72450|5|Briefly described|Brochure map|||||Burra Group|||Laminated dark grey and green siltstone.|
16502|Saddleworth Formation|73093|5|Briefly described|map legend|Neoproterozoic|Neoproterozoic||||||Mudstone, siltstone and shale, partly carbonaceous, dolomitic.|09-DEC-21
16502|Saddleworth Formation|73188|5|Briefly described|p316, p325-329, p331, p333, p340|Neoproterozoic|Neoproterozoic|Mount Lofty Ranges.||Bungarider Subgroup, Burra Group||Underlain by Stonyfell Quartzite.|Slate, dolomitic siltstone.|
16502|Saddleworth Formation|74367|6|Mentioned|p7 Fig.6|||||Bungarider Subgroup||||
16542|Saint Kilda Formation|23482|5|Briefly described|p9|Holocene|Holocene|Saint is St. in text.||||||
16542|Saint Kilda Formation|23489|5|Briefly described|p43 Table 1|Holocene|Holocene|Saint is St. in text.||||||
16542|Saint Kilda Formation|23719|4|Described|p32|Holocene|Holocene|Saint is St. in text. See also page 30 table 9. Overlain by Semaphore Sand. Underlain by Moornaba Sand. Geological Province: Gawler Craton [?unlikely].||||||04-NOV-10
16542|Saint Kilda Formation|23731|6|Mentioned|p23, p29|Holocene|Holocene|Saint is St. in text.||||||
16542|Saint Kilda Formation|23818|4|Described|p212 Fig.108, p224|Recent|Recent|Geological Province: Otway Basin. Saint is spelt St. in text. Overlying units: Fulham Sand and Semaphore Sand. Underlying unit: Pooraka Formation. Age: 1000-4000 years B.P.||||||
16542|Saint Kilda Formation|29697|6|Mentioned|Table 7|||||||||
16542|Saint Kilda Formation|30080|6|Mentioned|p2|||||||||
16542|Saint Kilda Formation|30752|6|Mentioned|Table 1|||||||||
16542|Saint Kilda Formation|30753|6|Mentioned|p15|||Recent||||||
16542|Saint Kilda Formation|30754|5|Briefly described|p22|||Stratigraphic table. Sections P28,36||||||
16542|Saint Kilda Formation|30756|6|Mentioned|p2|||||||||
16542|Saint Kilda Formation|30807|6|Mentioned|p101|||Suggested map symbol||||||
16542|Saint Kilda Formation|30922|6|Mentioned|Map legend|Holocene|Holocene|||||||
16542|Saint Kilda Formation|31655|6|Mentioned|Table 1|||Geology & hydrology||||||
16542|Saint Kilda Formation|31850|4|Described|p40|||||||||
16542|Saint Kilda Formation|31921|5|Briefly described|p6|||||||||
16542|Saint Kilda Formation|32438|6|Mentioned|p41|||||||||
16542|Saint Kilda Formation|33054|6|Mentioned|p53|||See also Fig.1||||||
16542|Saint Kilda Formation|33422|6|Mentioned|Map legend|Cenozoic|Cenozoic|||||||19-NOV-08
16542|Saint Kilda Formation|33423|6|Mentioned|p15|||Strat.||||||
16542|Saint Kilda Formation|34180|5|Briefly described|p224|||Recent. See P212||||||
16542|Saint Kilda Formation|34181|4|Described|p47|||Recent||||||
16542|Saint Kilda Formation|34295|6|Mentioned|p42|||Pleistocene. Fauna||||||
16542|Saint Kilda Formation|34536|6|Mentioned|Map legend|Recent|Recent|||||||
16542|Saint Kilda Formation|35028|6|Mentioned|p339|||||||||
16542|Saint Kilda Formation|35097|6|Mentioned|p27|||||||||
16542|Saint Kilda Formation|35159|5|Briefly described|p12|||See also Fig.2.||||||
16542|Saint Kilda Formation|35673|6|Mentioned|Fig.1|||Location plan, Para Hills quartzite quarry.||||||
16542|Saint Kilda Formation|35677|6|Mentioned|p54|||||||||
16542|Saint Kilda Formation|35772|6|Mentioned|Table 1|||||||||
16542|Saint Kilda Formation|36621|6|Mentioned|Fig.1|||||||||
16542|Saint Kilda Formation|36626|6|Mentioned|Fig.1|||||||||
16542|Saint Kilda Formation|36834|6|Mentioned|Fig.1|||||||||
16542|Saint Kilda Formation|36835|6|Mentioned|Fig.1|||||||||
16542|Saint Kilda Formation|36894|6|Mentioned|Fig.2|||||||||
16542|Saint Kilda Formation|37853|6|Mentioned|Fig.1|||||||||
16542|Saint Kilda Formation|38068|5|Briefly described|p79|||See also Fig.8.||||||
16542|Saint Kilda Formation|38107|6|Mentioned|Fig.2|||||||||
16542|Saint Kilda Formation|38699|6|Mentioned|p30|||||||||
16542|Saint Kilda Formation|38700|6|Mentioned|p42|||||||||
16542|Saint Kilda Formation|39349|6|Mentioned|Map legend|Holocene|Holocene|||||||
16542|Saint Kilda Formation|39351|6|Mentioned|Map legend|late Holocene|late Holocene|||||||
16542|Saint Kilda Formation|39835|4|Described|p281|||||||||
16542|Saint Kilda Formation|40003|5|Briefly described|Table 11|||||||||
16542|Saint Kilda Formation|40149|1|Redefined|p121|Holocene|Holocene|||||||
16542|Saint Kilda Formation|40219|6|Mentioned|p2|||||||||
16542|Saint Kilda Formation|40442|6|Mentioned|p38|||||||||
16542|Saint Kilda Formation|40448|6|Mentioned|p43|||||||||
16542|Saint Kilda Formation|40502|5|Briefly described|p83|||||||||
16542|Saint Kilda Formation|40556|6|Mentioned|p66|||||||||
16542|Saint Kilda Formation|40643|6|Mentioned|p149|||||||||
16542|Saint Kilda Formation|40941|6|Mentioned|Map legend|Holocene|Holocene|||||||
16542|Saint Kilda Formation|40942|4|Described|p23|||||||||
16542|Saint Kilda Formation|40976|5|Briefly described|p280|||||||||
16542|Saint Kilda Formation|41078|6|Mentioned|p47|||||||||
16542|Saint Kilda Formation|41151|6|Mentioned|p14|||||||||
16542|Saint Kilda Formation|41278|5|Briefly described|p110|||||||||
16542|Saint Kilda Formation|41292|6|Mentioned|Fig.1|||||||||
16542|Saint Kilda Formation|41362|5|Briefly described|p7|||||||||
16542|Saint Kilda Formation|41499|6|Mentioned|p70|||||||||
16542|Saint Kilda Formation|41506|6|Mentioned|p9|||||||||
16542|Saint Kilda Formation|41943|6|Mentioned|Fig.3 P73|||||||||
16542|Saint Kilda Formation|42498|5|Briefly described|Map legend|Holocene|Holocene|Actually spelt St Kilda Formation.||||||
16542|Saint Kilda Formation|42717|6|Mentioned|map legend|Holocene||Actually spelt St Kilda Formation||||||
16542|Saint Kilda Formation|42966|2|Defined|p286|Holocene||Actually spelt St Kilda Formation.||||||
16542|Saint Kilda Formation|43049|6|Mentioned|p28|||actually spelt St Kilda Formation||||||
16542|Saint Kilda Formation|43052|5|Briefly described|Table 2.1|||actually spelt St Kilda Formation||||||
16542|Saint Kilda Formation|43053|5|Briefly described|Map Legend|Holocene|Holocene|Spelt St Kilda Formation. Calcareous, fossiliferous sand and mud of intertidal flats, beaches and tidal marshes; organic, gypseous clay of supratidal flats.||||||25-MAY-05
16542|Saint Kilda Formation|43073|6|Mentioned|p17|||actually spelt St Kilda Formation||||||
16542|Saint Kilda Formation|43258|5|Briefly described|Map Legend||Holocene|Spelt St.Kilda Formation.||||||
16542|Saint Kilda Formation|44133|5|Briefly described|p220 Fig. 11.2|Holocene|Pleistocene|||||||
16542|Saint Kilda Formation|49038|4|Described|Table 2|||||||||
16542|Saint Kilda Formation|60953|5|Briefly described|Map Legend|Holocene|Holocene|Calcareous, fossiliferous sand and mud of intertidal sand flats, beaches and tidal marshes; organic, gypseous clay of supratidal flats.||||||
16542|Saint Kilda Formation|60958|5|Briefly described|Map Legend|Holocene|Holocene|Undifferentiated holocene coastal marine sediment. <7000 yrs to present.||||||12-MAR-09
16542|Saint Kilda Formation|61070|5|Briefly described|Map Legend|Holocene|Holocene|Coastal sediments.||||||12-JAN-10
16542|Saint Kilda Formation|61108|5|Briefly described|map legend|Holocene|Holocene|Spelt St. on map legend. Calcareous, fossiliferous sand and mud of intertidal sand flats, beaches and tidal marshes; organic, gypseous clay of supratidal flats.||||||
16542|Saint Kilda Formation|61121|5|Briefly described|Map legend|Holocene|Holocene|Comprises three members and undifferentiated Holocene coastal marine sediment. members: Le Hunte, Semaphore Sand and Gantheaume Sand Members. Saint is St in text of legend.||||||07-JUN-05
16542|Saint Kilda Formation|62893|4|Described|Map Legend, p25|Holocene|Holocene|Reflects an intertidal setting. Facies equivalent of Semaphore Sand and Yamba Formation [not necessarily a stratigraphic equivalent].|ca 0.0066 Ma||||Shelly mud and sand, and stranded beach sand.|
16542|Saint Kilda Formation|63124|6|Mentioned|p93|||Geological Province: Gambier Basin. Saint is St in text.||||||
16542|Saint Kilda Formation|64282|5|Briefly described|Map legend|Holocene|Holocene|Includes Gantheaume and Semaphore Sand Members, and le Hunte Member, plus undifferentiated coastal marine sediment.  Age <7000years to present. Saint is St in legend.||||||24-JUL-08
16542|Saint Kilda Formation|65901|6|Mentioned|p177|Holocene|Holocene|Interfingers with Waldeila Formation. Marine.||||||08-MAR-12
16542|Saint Kilda Formation|68131|6|Mentioned|p12, p31|Holocene|Holocene|SW Yorke Peninsula.||||||
16542|Saint Kilda Formation|68811|5|Briefly described|p85, p86|||Deposited in an estuarine setting. Hosts good quality water that is recharged periodically by rainwater.|||Includes the Semaphore Sands.||Muds and silts.|
16542|Saint Kilda Formation|69048|5|Briefly described|p2|Cenozoic|Cenozoic|Southern Eyre Peninsula.|||Semaphore Sand Member.|||
16542|Saint Kilda Formation|69666|6|Mentioned|p25, p27|Cenozoic|Cenozoic|||||||
16542|Saint Kilda Formation|70334|5|Briefly described|p3,61-62,65,70-71,73,90-91,93|Holocene|Holocene|Of Spencer Gulf area. Peritidal sediments. Part of a prograding cool water carbonate platform extending along the southern margin of Australia (Gostin et al., 1984a, Gostin et al., 1988).||||Disconformably overlies the Lowly Point Formation and the Mambray Formation.|Subtidal seagrass banks, shallow channels and mega-ripple fields, intertidal sand flats, mangrove-algal and halophyte-algal marshes, supratidal sand flats, sabkhas, stranded beach ridges and coastal dunes.|14-OCT-19
16542|Saint Kilda Formation|73103|5|Briefly described|Map legend.|Holocene|Holocene||||||Undifferentiated Holocene coastal marine sediment.|
16542|Saint Kilda Formation|73107|5|Briefly described|Map legend.|Holocene|Holocene|Appears on the map as ST KILDA FORMATION.|<7000 yrs to present.||||Undifferentiated Holocene coastal marine sediment.|
16542|Saint Kilda Formation|73110|5|Briefly described|Map legend.|Holocene|Holocene||||||Undifferentiated Holocene coastal marine sediment.|
16542|Saint Kilda Formation|73188|6|Mentioned|p320|Holocene|Holocene|[Written as St Kilda Formation]. St Vincent Basin.|||Semaphore Sand Member||Muddy and sandy coastal sediments.|
16542|Saint Kilda Formation|73236|5|Briefly described|p36, p38, p44|Holocene|Holocene|Coastal sediments; beach and dune sands. Represents shoreline deposits of the Holocene transgression in South Australia.|||Semaphore Sand Member|||
16542|Saint Kilda Formation|73302|6|Mentioned|p34|Holocene|Holocene|||||||
16579|Samuel Formation|7433|5|Briefly described|p25 Fig.2, p42, p47.|Aptian|Aptian|Canning Basin and, more extensively, Officer Basin. Marine fine clastics. Contains pelecypods, gastropods and palynomorphs.||||Laterally equivalent to Anketell Sandstone. Underlies Bejah Claystone.|Thin-bedded, shallow-marine, fine sandstone and mudstone.|
16579|Samuel Formation|22707|6|Mentioned|P16|||||||||
16579|Samuel Formation|22753|5|Briefly described|Fig.3 p585|Cretaceous|Cretaceous|||||||
16579|Samuel Formation|22801|6|Mentioned|P13||Early Cretaceous|Equivalent to the Anketell Sandstone||||||
16579|Samuel Formation|22814|5|Briefly described|fig2|Cretaceous|Cretaceous|||||||
16579|Samuel Formation|24067|5|Briefly described|p252|Aptian|Aptian|Geological Province: Officer Basin.||||||
16579|Samuel Formation|24161|5|Briefly described|p28|Early Cretaceous|Early Cretaceous|Unconformably overlies the Paterson Formation.||||||
16579|Samuel Formation|31153|6|Mentioned|p111|||Refers bivalves of Offices Basin||||||
16579|Samuel Formation|31455|4|Described|Table 2|||||||||
16579|Samuel Formation|31456|4|Described|Table 1|||||||||
16579|Samuel Formation|31459|6|Mentioned|Map legend|Mesozoic|Mesozoic|||||||
16579|Samuel Formation|31632|4|Described|Table 2|||See also p12.||||||09-FEB-18
16579|Samuel Formation|31633|4|Described|Table 2|||||||||
16579|Samuel Formation|31635|4|Described|Table 2|||||||||
16579|Samuel Formation|31636|5|Briefly described|p7|||See also Table 2||||||
16579|Samuel Formation|31638|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16579|Samuel Formation|31639|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16579|Samuel Formation|31640|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16579|Samuel Formation|31642|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16579|Samuel Formation|31914|2|Defined|p98|Aptian|Aptian|||||||
16579|Samuel Formation|33587|3|Fully described|p9|||Table 2.||||||
16579|Samuel Formation|33588|4|Described|p9|||Table 2.||||||
16579|Samuel Formation|33595|6|Mentioned|p16|||||||||
16579|Samuel Formation|33596|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16579|Samuel Formation|33597|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16579|Samuel Formation|35127|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16579|Samuel Formation|35222|4|Described|Table.2|||||||||
16579|Samuel Formation|35223|6|Mentioned|Table.2|||||||||
16579|Samuel Formation|35250|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16579|Samuel Formation|35387|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16579|Samuel Formation|35497|6|Mentioned|Table 1|||||||||
16579|Samuel Formation|35902|4|Described|Table 1|||||||||
16579|Samuel Formation|35903|4|Described|Table 1|||||||||
16579|Samuel Formation|36257|6|Mentioned|Table 2.1|||||||||
16579|Samuel Formation|36701|6|Mentioned|Map legend|Early Cretaceous|Early Permian|Early Cretaceous to Early Permian||||||
16579|Samuel Formation|36890|3|Fully described|p353|||See also p406.||||||10-FEB-20
16579|Samuel Formation|37916|5|Briefly described|Fig.2|||||||||
16579|Samuel Formation|38878|6|Mentioned|Map legend|Albian|Aptian|Albian - Aptian||||||
16579|Samuel Formation|38898|6|Mentioned|Table 1|||||||||
16579|Samuel Formation|39211|5|Briefly described|p53|||||||||
16579|Samuel Formation|42194|6|Mentioned|p8|||||||||
16579|Samuel Formation|42431|5|Briefly described|p237|||||||||
16579|Samuel Formation|42734|5|Briefly described|map legend|Cretaceous||||||||
16579|Samuel Formation|43563|6|Mentioned|Fig2,p5||Early Cretaceous|||||||
16579|Samuel Formation|43656|6|Mentioned|Fig.2,p8|Aptian|Barremian|||||||
16579|Samuel Formation|43746|6|Mentioned|Fig.2,p11|Aptian|Barremian|||||||
16579|Samuel Formation|44145|6|Mentioned|p553|||Officer Basin rocks. Must be Early Cretaceous (age of Madura Formation)||||To south, grade laterally into Madura Formation.||
16579|Samuel Formation|44354|5|Briefly described|Map Legend||Early Cretaceous|||||||
16579|Samuel Formation|45104|5|Briefly described|p30|||||||||
16579|Samuel Formation|45149|2|Defined|p53|Early Cretaceous|Early Cretaceous|See also table 1 and P9.||||||
16579|Samuel Formation|45153|2|Defined|App.8-140|Aptian|Aptian|||||||
16579|Samuel Formation|45158|3|Fully described|p12|||||||||
16579|Samuel Formation|45168|6|Mentioned|p6, Table 1|||||||||
16579|Samuel Formation|46975|6|Mentioned|p86|||||||||
16579|Samuel Formation|64580|4|Described|map legend||Early Cretaceous|Siltstone, sandstone and claystone; micaceous, carbonaceous; locally glauconitic.||||||09-DEC-08
16579|Samuel Formation|64643|5|Briefly described|p3 Fig. 2|Early Cretaceous|Early Cretaceous|||||||10-FEB-20
16579|Samuel Formation|64970|6|Mentioned|p719 Fig. 2|Cretaceous|Jurassic|Geological Province: Officer Basin.||||||27-MAY-09
16579|Samuel Formation|65102|4|Described|p366,369,374, Figure 4-41, p369|Aptian|Valanginian|Officer Basin. 2-80m; variegated siltstone, sandstone & claystone; micaceous, carbonaceous & glauconitic beds; marine, shallow water; disconformable on Paterson Formation; type section at Mount Charles, 25deg 46min S, 125deg 06min E.||||||
16579|Samuel Formation|65301|5|Briefly described|p5 Fig. 4|Early Cretaceous|Early Cretaceous|Geological province: Canning Basin.||||||
16579|Samuel Formation|65416|5|Briefly described|p144.|Cretaceous|Cretaceous|Central and northwest Officer Basin.|||||Thin unit of interbedded marine sandstones and claystones.|
16579|Samuel Formation|65449|6|Mentioned|p6|Early Cretaceous|Early Cretaceous|||||Overlies Callawa and Cronin Formations. Is overlain by Bejah Claystone.||
16579|Samuel Formation|67195|4|Described|p19 table 1, p45, 46, 47|||Western Officer Basin. Thermal conductivity of 1.28 W/mK. See also App 1, App 2.|||||Grey to yellow laminated claystone, siltstone and fine grained sandstone; sulphurous, occasional bioturbation, micaceous glauconite?; reddish brown to ochre siltstone, claystone with finely laminated interbeds of whispy fine-grained sandstone.|
16579|Samuel Formation|67200|5|Briefly described|app 2 p10||||||||Laminated claystone, siltstone and fine grained sandstone; sulphorous and occasionally bioturbated.|
16579|Samuel Formation|68007|6|Mentioned|p4, p8|Early Cretaceous|Early Cretaceous|Canning Basin. Barremian to Aptian.||||(Most probably) overlies Callawa Formation.||19-FEB-20
16579|Samuel Formation|68902|6|Mentioned|p9 fig 5|Cretaceous|Cretaceous|||||Overlies Callawa and Cronin Formations; is overlain by Bejah Claystone.||
16579|Samuel Formation|69029|6|Mentioned|p319|Aptian|Barremian|Of Canning Basin.||||Overlain by Baja Claystone. Underlain by Broome Sandstone.||
16579|Samuel Formation|69091|6|Mentioned|p106 Fig.5.7a, see comments|||See also p107 Fig.5.8a, p109 Fig.5.10.||||||
16579|Samuel Formation|69153|6|Mentioned|500k_geologyp08_lut.csv||Early Cretaceous|Lithology description shared with Bejah Claystone|||||Siltstone, sandstone and claystone; micaceous, carbonaceous|
16579|Samuel Formation|69182|6|Mentioned|Ch4 p9, Ch4 p45, Ch4 p47|Early Cretaceous|Early Cretaceous|Canning Basin.||||Overlies the Callawa and Cronin Formations. Overlain by the Bejah Claystone.||10-FEB-20
16579|Samuel Formation|69312|5|Briefly described|p3|Aptian|Barremian|Canning Basin.||||Overlies the Broome and Barbwire Sandstones. Overlain by the Baja Claystone.|Shale and sandstone.|
16579|Samuel Formation|70634|4|Described|500k_geolgyp08_lut.csv|Early Cretaceous|Early Cretaceous|Included with Bejah Claystone in file (undivided)|||||undivided; siltstone, sandstone and claystone; micaceous, carbonaceous; locally glauconitic, radiolarian siltstone in Bejah Claystone|09-FEB-18
16579|Samuel Formation|70774|5|Briefly described|p4|Early Cretaceous|Early Cretaceous|Willara and Kidson Sub-basins, Canning Basin.||||Overlies the Callawa and Cronin Formations. Overlain by the Bejah Claystone.||10-FEB-20
16579|Samuel Formation|70793|4|Described|500k_interpgeop14_lut.csv|Albian|Aptian|Of Gunbarrel Basin. Events: Timorese Collision (20-0.01 Ma); Gondwana breakup-southern margin (100.5-93.9 Ma); Aptian transgression (123-121 Ma). See 500k_interpgeop14_lut.csv, 2_5m_interpgeop15_lut.csv.|125-100.5 Ma (biostrat)||||Siltstone, sandstone and claystone; carbonaceous, locally glauconitic; radiolarian siltstone in Bejah Claystone|
16579|Samuel Formation|70826|6|Mentioned|p7 tbl 4|Cretaceous|Cretaceous|Gunbarrel Basin.||||||
16579|Samuel Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone, claystone, siltstone|
16579|Samuel Formation|71268|4|Described|GEOL_LUT_CSV files|Albian|Aptian|Of Gunbarrel Basin. Events: Timorese Collision (20-0.01 Ma); Gondwana breakup-southern margin (100.5-93.9 Ma); Aptian transgression (123-121 Ma). See 1m_geologyp12_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv.|125-100.5 Ma (biostrat)|||Correlable with Bejah Claystone.|Siltstone, sandstone and claystone; micaceous, carbonaceous; locally glauconitic.|
16579|Samuel Formation|72034|6|Mentioned|500k_interpgeop16_lut|Albian|Aptian|Gunbarrel Basin. Shown as informal combination with Bejah Claystone.  Age from biostratigraphy.||||||
16579|Samuel Formation|72497|5|Briefly described|p3 Fig.2.|Aptian|Barremian|Shown as occuring in the Anketell, Tabletop, Ryan Shelves, Willara and Kidson Sub-basins.||||Conformably overlies Cronin and Callawa Formation and underlies Bejah Claystone. Laterally equivalent to Melligo-Para-Frozier Sandstone.||
16579|Samuel Formation|72499|5|Briefly described|p7 Fig.6.|Early Cretaceous|Early Cretaceous|Located in the Willara Sub-basin and the Broome Platform.||||Overlies Callawa and Cronin Formations and partially overlies Broome Sandstone. Laterally equivalent to Frezier Sandstone.|Includes shale.|
16579|Samuel Formation|73117|5|Briefly described|p3|Lower Cretaceous|Lower Cretaceous|Canning Basin.||||Underlain by Callawa/Cronin formations. Overlain by Bejah Claystone. Equivalent to Frezier Sandstone, Parda Formation, and Melligo Sandstone.|Dominantly shale and mudstone.|
16579|Samuel Formation|73346|6|Mentioned|p28|Cretaceous|Cretaceous|Ryan Shelf.||||Unconformably underlain by Grant Group.||
16581|San Marino Paleosol|38602|6|Mentioned|Fig.2|||||||||
16735|Sellick Hill Formation|22581|6|Mentioned|Fig.2,p37|||Normanville Group, Kanmantoo Basin. Overlain by Fork Tree Limestone||||||
16735|Sellick Hill Formation|22643|5|Briefly described|fig3p187|Early Cambrian|Early Cambrian|||||||
16735|Sellick Hill Formation|22766|4|Described|Fig.2 p561, p562|Early Cambrian|Early Cambrian|||||||
16735|Sellick Hill Formation|23981|5|Briefly described|p8-9 Fig. 4, p10 Fig. 5|Early Cambrian|Early Cambrian|Supersedes Sellick Hill Limestone. Consists of 5 facies (named facies asocciations A-E in ascending order of Alexander and Gravestock, 1990). Overlies Wangkonda Formation; underlies Fork Tree Limestone. Max. thickness: 84m. Geol.Prov: Stansbury Basin.||||||04-FEB-08
16735|Sellick Hill Formation|24465|6|Mentioned|p358|Early Cambrian|Early Cambrian|Of Normanville Group.  Geological Province: Stansbury Basin.||||||19-JAN-05
16735|Sellick Hill Formation|33953|6|Mentioned|Fig.4|||Cambrian||||||
16735|Sellick Hill Formation|35255|6|Mentioned|Fig.8|||||||||
16735|Sellick Hill Formation|38873|6|Mentioned|Table 2|||||||||
16735|Sellick Hill Formation|39806|6|Mentioned|p207|||||||||
16735|Sellick Hill Formation|40442|5|Briefly described|p15|||||||||
16735|Sellick Hill Formation|40455|5|Briefly described|p67|||||||||
16735|Sellick Hill Formation|40852|6|Mentioned|p33|||||||||
16735|Sellick Hill Formation|41103|6|Mentioned|Fig.1|||||||||
16735|Sellick Hill Formation|41526|6|Mentioned|p61|||||||||
16735|Sellick Hill Formation|42192|6|Mentioned|p6|||||||||
16735|Sellick Hill Formation|42222|6|Mentioned|Table 1 P4|||||||||
16735|Sellick Hill Formation|42225|6|Mentioned|Fig.4 P224|||||||||
16735|Sellick Hill Formation|42232|6|Mentioned|p269|||||||||
16735|Sellick Hill Formation|42266|5|Briefly described|p291|||||||||
16735|Sellick Hill Formation|42270|6|Mentioned|p353|||||||||
16735|Sellick Hill Formation|42458|6|Mentioned|p702|||||||||
16735|Sellick Hill Formation|43703|6|Mentioned|Fig.1,p75|||||||||
16735|Sellick Hill Formation|44133|5|Briefly described|p4 Fig. 7.2, 6, 8, 9|Early Cambrian|Early Cambrian|Geological Province: Stansbury Basin. Of the Normanville Group.||||||
16735|Sellick Hill Formation|60712|5|Briefly described| p28 Fig. 1|Early Cambrian|Early Cambrian|Of the Normanville Group.||||||31-MAY-05
16735|Sellick Hill Formation|63848|6|Mentioned|p534 Fig.4.|||||Unit in Normanville Group.||Overlies Wangkonda Formation. Is overlain by Fork Tree Limestone.||
16735|Sellick Hill Formation|65375|5|Briefly described|p33.|Early Cambrian|Early Cambrian|||Unit in Normanville Group.||Overlies Wangkonda Formation. Is overlain by Fork Tree Limestone.||
16735|Sellick Hill Formation|65686|6|Mentioned|p420|Cambrian|Cambrian|||||||
16735|Sellick Hill Formation|65892|5|Briefly described|p9 Fig.4, p14-19. |Early Cambrian|Early Cambrian|Fleurieu Peninsula. 210m thick. Poorly-preserved hyoliths are concentrated in pockets of the cut and fill structure where it overlies the Wangkonda Formation. Shows a variety of depositional facies. Fossiliferous.||Unit in Normanville Group.||Disconformably overlies Wangkonda Formation. Is overlain conformably by Fork Tree Limestone.|Coarse arkose, calcarenite, minor siltstone; interbedded sand, silt and shale with abundant bioturbation; interbedded limestones and calcareous shales, minor conglomerate; biohermal packstone; ribbon limestone with isolated bioherms.|
16735|Sellick Hill Formation|66761|6|Mentioned|p254|Cambrian|Cambrian|Fleurieu Peninsula. Younger than Wangkonda Formation, older than Fork Tree Limestone.||||||
16735|Sellick Hill Formation|68735|6|Mentioned|p233 Fig.2, p235 Fig.3|Early Cambrian|Early Cambrian|Stansbury Basin.||Of the Normanville Group.||||
16735|Sellick Hill Formation|68993|6|Mentioned|p544 Fig.1|Early Cambrian|Early Cambrian|Fleurieu Peninsula.||Of the Normanville Group.||||
16735|Sellick Hill Formation|70660|5|Briefly described|p40|Early Cambrian|Early Cambrian|||||||
16735|Sellick Hill Formation|70833|5|Briefly described|p200,202|Cambrian|Cambrian|Of Eastern Stansbury Basin. Includes K. rostrata zone in the uppermost part of the section. Equivalent to lower parts of Wilkawillina and Wirrapowie and Ajax limestones.||||Overlain by Fork Tree Limestone. Underlain by Wankonda Formation.||
16735|Sellick Hill Formation|72450|5|Briefly described|Brochure map||||c. 520 Ma|Normanville Group|||Dakr grey,ribboned, silty limestone.|
16735|Sellick Hill Formation|73188|6|Mentioned|p316|Early Cambrian|Early Cambrian|Mount Lofty Ranges.||Normanville Group|||Thin-bedded silty limestone.|
16735|Sellick Hill Formation|73247|6|Mentioned|p205|Cambrian (Stage 2)|Cambrian (Stage 2)|Fleurieu Peninsula.||||Unconformably underlain by Wangkonda Formation. Overlain by Fork Tree Limestone. Equivalent to Kulpara Formation.||
16761|Serle Conglomerate|22510|5|Briefly described|table1p36,41|||Formerly Serle Conglomerate Member of Tapley Hill Formation.||||||31-JUL-13
16761|Serle Conglomerate|24176|5|Briefly described|p11|||Of Yudnamutana Sub-Group (Umberatana Group). Overlies Lyndhurst Formation unconformably. Geological Province: Mount Painter Province.||||||13-FEB-08
16761|Serle Conglomerate|24321|5|Briefly described|Map legend|Adelaidean|Adelaidean|Parent: Umberatana Group.||||||13-FEB-08
16761|Serle Conglomerate|30178|6|Mentioned|p20|||||||||
16761|Serle Conglomerate|37238|6|Mentioned|p368|||||||||
16761|Serle Conglomerate|37932|5|Briefly described|p539|||||||||
16761|Serle Conglomerate|41364|6|Mentioned|p167|||||||||
16761|Serle Conglomerate|41405|3|Fully described|p152|||Type section: occurs as an apparently lenticular unit between 1.3 and 6.5 km northeast of Tindelpina Hut, and Coats and Blissett (1971) specified a type section at latitude 30degrees04'56"S, longitude 139degrres18'21"E to latitude 30degrees04'27"S, longitude 139degrees19'02"E, with a thickness of 305 m.||||||26-NOV-22
16761|Serle Conglomerate|41647|6|Mentioned|Fig.2|||||||||
16761|Serle Conglomerate|41770|4|Described|p238|||||||||
16761|Serle Conglomerate|42222|5|Briefly described|p16|||||||||
16761|Serle Conglomerate|43052|5|Briefly described|p183,Table 6.1|||of Umberatana Group||||||
16761|Serle Conglomerate|60718|5|Briefly described|p49 Fig. 2, p53, 55|Adelaidean|Adelaidean|Geological Province: Adelaide Geosyncline. See also p51 Fig. 3.||Of Nepouie Subgroup (Umberatana Group).||Gradationally(?) underlies Tindelpina Shale Member (Tapley Hill Formation). Unconformably overlies Wilyerpa Formation.||15-APR-11
16761|Serle Conglomerate|67979|6|Mentioned|p529|||Serle Conglomerate Member intended?  Name used interchangeably with Serle Conglomerate Member on p529, but Member implied with first use.||||||
16761|Serle Conglomerate|69019|4|Described|p46-47, p162-163.|Neoproterozoic|Neoproterozoic|Coats et al. (1969) separated this from Tapley Hill Formation as a distinct unit; Preiss (1987) formalised it as a Formation. Text (p163) says that 'Yudnamutana Subgroup...unconformably underlies the Serle Conglomerate'. Only occurs within Willouran Ranges. Thickness to c.300 m. Hosts copper mineralisation at Breaden Hill and Boorloo areas.|||Unit in Yudnamutana Subgroup(?)|Overlain gradationally by Tapley Hill Formation.|Lenticular pebbly greyish gritty sandstone with lenses of well-bedded to finely laminated carbonaceous shale.|
16761|Serle Conglomerate|70384|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Adelaide Geosyncline.  Age shown more specifically as Sturtian [Cryogenian].||Nepouie Subgroup.||Is overlain by Tindelpina Shale Member (Tapley Hill Formation).|Greyish, gritty pebbly sandstone; well-bedded carbonaceous shale.|21-JAN-19
16761|Serle Conglomerate|72456|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Marree 1:250k map sheet.|||||Conglomerate, grit, carbonaceous shale.|
16795|Shanahan Conglomerate Member|22631|6|Mentioned|p177|||||||||
16795|Shanahan Conglomerate Member|22772|5|Briefly described|Table13.1|Cryogenian|Cryogenian|||||||
16795|Shanahan Conglomerate Member|22857|5|Briefly described|Tb. 13.1 (insert p70-71)|Willouran|Willouran|Of the Paralana Quartzite (Arkaroola Subgroup, Callanna Group).||||||
16795|Shanahan Conglomerate Member|23394|5|Briefly described|Map legend|Proterozoic|Proterozoic|||||||
16795|Shanahan Conglomerate Member|24176|6|Mentioned|p26 Tb. 1|Adelaidean|Adelaidean|Age is Willouran. Geological Province: Mount Painter Province.||||||12-NOV-13
16795|Shanahan Conglomerate Member|30177|2|Defined|p126|Adelaidean|Adelaidean|See also p50. Type area: 1.4 miles east-northeast of Greenhill Hut, lat. 30degrees05'17" S long.139degrees22'24"E.||||||25-NOV-22
16795|Shanahan Conglomerate Member|30801|6|Mentioned|p5|||Paralana Quartzite. Table P5-6.||||||
16795|Shanahan Conglomerate Member|30807|6|Mentioned|p103|||Suggested map symbol||||||
16795|Shanahan Conglomerate Member|40294|6|Mentioned|Table 2|||||||||
16795|Shanahan Conglomerate Member|41403|5|Briefly described|p46|||||||||
16795|Shanahan Conglomerate Member|42624|5|Briefly described|p20|||||||||
16795|Shanahan Conglomerate Member|43052|5|Briefly described|Table 6.1|||of Paralana Quartzite||||||
16795|Shanahan Conglomerate Member|65338|6|Mentioned|p59.|||Adelaide Fold Belt. Considered by Walter and Veevers (2000) to correlate with Vaughan Springs Quartzite.||Basal unit in Paralana Quartzite.||||
16795|Shanahan Conglomerate Member|68068|5|Briefly described|Map legend|Willouran|Willouran|Basal unconformity.||Unit in Paralana Quartzite.|||Rounded quartzite cobbles with magnetite and pyrite-rich quartzite matrix.|12-NOV-14
16795|Shanahan Conglomerate Member|69023|6|Mentioned|p61-62|Neoproterozoic|Neoproterozoic|||Unit in Paralana Quartzite.||||
16795|Shanahan Conglomerate Member|70384|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Adelaide Geosyncline. The base rests on a major unconformity surface. Age shown more specifically as Willouran [basal Cryogenian].||Of Paralana Quartzite.|||Consists of rounded quartzite cobbles with magnetite and pyrite-rich quartzite matrix. Interdigitates with the main quartzite and in some locations forms two or three ~1m thick basal beds.|18-JAN-19
16795|Shanahan Conglomerate Member|73222|6|Mentioned|p7|Tonian|Tonian|Adelaide Rift Complex, Gammon Ranges. Willouran.||Arkaroola Subgroup, Callanna Group, Warrina Supergroup||Overlain by [?]Paralana Quartzite.||
16797|Shannon Formation|9199|5|Briefly described|Map legend|Cambrian|Cambrian|Of the Pertaoorrta Group.  Siltstone, shale, limestone, dolomite; fossiliferous.  Geological Province: Amadeus Basin.||||||04-NOV-04
16797|Shannon Formation|12891|5|Briefly described|p732|Middle Cambrian|Middle Cambrian|Geological province: Amadeus Basin. Lithology possibly analogous with Point Wakefield beds in Wiso Basin.||||||07-FEB-11
16797|Shannon Formation|22561|5|Briefly described|p21|Neoproterozoic|Neoproterozoic|In the Ooraminna Sub-basin.||||||30-NOV-06
16797|Shannon Formation|22566|5|Briefly described|p85|Late Cambrian|Middle Cambrian|Of the Pertaoorrta Group.  Informally divided into upper and lower Shannon Formation.||||||30-NOV-06
16797|Shannon Formation|22646|6|Mentioned|p 104|Cambrian|Cambrian|||||||
16797|Shannon Formation|22650|6|Mentioned|p 159|Cambrian|Cambrian|of the Pertaoorrta Group.||||||30-NOV-06
16797|Shannon Formation|22651|4|Described|p 186 - 187|Late Cambrian|Middle Cambrian|Of the Pertaoorrta Group.  Informally divided into upper and lower Shannon Formation p 171.||||||30-NOV-06
16797|Shannon Formation|22655|5|Briefly described|p 257|||||||||
16797|Shannon Formation|22656|5|Briefly described|p 281||Middle Cambrian|||||||
16797|Shannon Formation|22762|5|Briefly described|p369|Cambrian|Cambrian|Informally divided into upper and lower Shannon Formation.||||||30-NOV-06
16797|Shannon Formation|22804|6|Mentioned|Fig 2 on p432|Cambrian|Cambrian|Of the Pertaoorrta Group.||||||30-NOV-06
16797|Shannon Formation|22805|6|Mentioned|p464||Early Cambrian|||||||
16797|Shannon Formation|22826|4|Described|p572|Late Cambrian|Late Cambrian|||||||
16797|Shannon Formation|23361|5|Briefly described|16 Fig.4|Cambrian|Neoproterozoic III|||||||
16797|Shannon Formation|29721|6|Mentioned|Table 44|||||||||
16797|Shannon Formation|30258|6|Mentioned|Fig.2|||Part of Pertaoorta Group.||||||
16797|Shannon Formation|30544|6|Mentioned|p48|||Map legend||||||
16797|Shannon Formation|31572|6|Mentioned|Fig.|||Correlation chart. U.Camb.||||||
16797|Shannon Formation|33307|6|Mentioned|Fig.6|||||||||
16797|Shannon Formation|33761|6|Mentioned|p146|||Cambrian. Of the Pertaoorrta Formation.||||||30-NOV-06
16797|Shannon Formation|34111|5|Briefly described|Table 2|||Cambrian||||||
16797|Shannon Formation|34579|4|Described|Table 2|||Cambrian||||||
16797|Shannon Formation|35088|6|Mentioned|Fig.2|||||||||
16797|Shannon Formation|35102|6|Mentioned|Fig.2|||||||||
16797|Shannon Formation|35805|6|Mentioned|Fig.3|||||||||
16797|Shannon Formation|36198|6|Mentioned|p294|||See also Fig.III.2 and also p277.||||||30-NOV-06
16797|Shannon Formation|38606|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
16797|Shannon Formation|38885|6|Mentioned|Map legend|Late Cambrian|Late Cambrian|||||||
16797|Shannon Formation|39210|5|Briefly described|p38|||||||||
16797|Shannon Formation|39213|6|Mentioned|Fig.6|||Amadeus Basin Succession||||||
16797|Shannon Formation|39583|6|Mentioned|Map legend|Late Cambrian|Late Cambrian|||||||
16797|Shannon Formation|39931|6|Mentioned|Map legend|Cambrian|Cambrian|Of Pertaoorrta Group.||||||
16797|Shannon Formation|40254|6|Mentioned|Fig.7|||||||||
16797|Shannon Formation|40740|3|Fully described|p40|||Mention p5.||||||30-NOV-06
16797|Shannon Formation|40810|4|Described|p6|||||||||
16797|Shannon Formation|40906|6|Mentioned|Fig.11|||||||||
16797|Shannon Formation|40998|6|Mentioned|Fig.1|||||||||
16797|Shannon Formation|41018|6|Mentioned|Fig.2|||||||||
16797|Shannon Formation|41039|6|Mentioned|Fig.2|||||||||
16797|Shannon Formation|41115|6|Mentioned|Fig.2|||||||||
16797|Shannon Formation|41190|6|Mentioned|Fig.4|||||||||
16797|Shannon Formation|41224|6|Mentioned|Fig.2|||||||||
16797|Shannon Formation|41270|6|Mentioned|p274|||See also Table 1||||||
16797|Shannon Formation|41717|6|Mentioned|Fig.2|||||||||
16797|Shannon Formation|42059|6|Mentioned|Fig.2 P131|||||||||
16797|Shannon Formation|42060|6|Mentioned|p145|||||||||
16797|Shannon Formation|42082|6|Mentioned|Fig.3 P323|||||||||
16797|Shannon Formation|42354|5|Briefly described|Fig.4 P7|||||||||
16797|Shannon Formation|42504|5|Briefly described|p84|||In the Amadeus Basin.||||||30-NOV-06
16797|Shannon Formation|42886|5|Briefly described|Fig.1 P218|||||||||
16797|Shannon Formation|42940|5|Briefly described|Plate 12|||||||||
16797|Shannon Formation|43503|6|Mentioned|11-50|Mindyallan|Floran|||||||
16797|Shannon Formation|43646|6|Mentioned|Fig.3,p554||Middle Cambrian|||||||
16797|Shannon Formation|43781|6|Mentioned|p4||Late Cambrian|||||||
16797|Shannon Formation|43817|5|Briefly described|p61-63|||||||||
16797|Shannon Formation|44335|4|Described|p.11||Cambrian|Table 2. p.10.||||||
16797|Shannon Formation|44336|14|Not recorded|map legend||Cambrian|SG/53-3. Part of the Pertaoorrta Group.||||||30-NOV-06
16797|Shannon Formation|44433|14|Not recorded|map legend||Cambrian|||||||
16797|Shannon Formation|45041|4|Described|p57|||M-U Cambrian. Refers Wells et al. (1967)||||||
16797|Shannon Formation|45148|6|Mentioned|Fig.4|||In the Amadeus Basin.||||||30-NOV-06
16797|Shannon Formation|48890|2|Defined|p.40||Cambrian|See also Tables, Figs and Plates. Of the Pertaoorrta Group.||||||30-NOV-06
16797|Shannon Formation|48963|6|Mentioned|Fig.3|||||||||
16797|Shannon Formation|50246|5|Briefly described|p20 Fig. 2|Cambrian|Cambrian|Siltstone, shale, limestone and dolostone, well-interbedded, fossiliferous and stromatolitic.||||||07-FEB-11
16797|Shannon Formation|60547|5|Briefly described|Map Legend|Cambrian|Cambrian|Of the Pertaoorrta Group. Siltstone, shale, limestone, dolomite; fossiliferous. Geological Province: Amadeus Basin.||||||03-JUN-05
16797|Shannon Formation|61732|5|Briefly described|p99|Cambrian|Cambrian|Together with other Cambrian units overlies the Arumbera Sandstone.||||||07-FEB-11
16797|Shannon Formation|62376|5|Briefly described|p18|Late Cambrian|Middle Cambrian|Of the Pertaoorrta Group. Geological Province: Amadeus Basin.||||||09-FEB-10
16797|Shannon Formation|62379|5|Briefly described|p7 Fig. 2, p15|Late Cambrian|Middle Cambrian|Of the Pertaoorrta Group. Geological Province: Amadeus Basin. Siltstone, limestone, dolostone.||||||
16797|Shannon Formation|62595|5|Briefly described|p29 Fig.6.|Cambrian|Cambrian|Ross River area.|||||Siltstone, shale, limestone and dolostone, well interbedded, fossiliferous and stromatolitic.|
16797|Shannon Formation|63562|6|Mentioned|p338 fig 3,p346 fig 8, p348,p352 fig 10|Late Cambrian|Middle Cambrian|Of Amadeus Basin.||||Overlies Giles Creek Dolomite. Correlated with Arrinthrunga Formation. Is overlain by Goyder Formation.||
16797|Shannon Formation|64068|6|Mentioned|p65,67, 69, 70, 225|||Amadeus Basin. In part correlated with Steamboat Sandstone, Selwyn Range Limestone. Upper part correlated with Chabalowe Formation, Arrinthrunga Formation, Georgina Limestone.||||||
16797|Shannon Formation|64625|5|Briefly described|p244-245, p251|Cambrian|Cambrian|Amadeus Basin||||Overlies Giles Creek Dolomite|Siltstone, limestone and dolostone.|
16797|Shannon Formation|64778|6|Mentioned|p13|Cambrian|Cambrian|Amadeus Basin.||||||
16797|Shannon Formation|64809|5|Briefly described|p2, p3 Fig.2, p15 Fig.15 |Late Cambrian|Middle Cambrian|||Unit in Pertaoorrta Group.|||Siltstone, shale, limestone.|
16797|Shannon Formation|65233|3|Fully described|p3 Fig. 2, p8|Late Cambrian|Middle Cambrian|Of Pertaoorrta Gp. Conformable on/gradational with Giles Creek Dolostone. Max.thick: >700m, thinning to N and W. Geol.prov: Amadeus Basin. Lower part is silty shale with siltstone/dolostone thin interbeds; upper part is carbonate-rich - more lith. incl.||||||07-FEB-11
16797|Shannon Formation|65342|6|Mentioned|p4.|||Amadeus Basin. Max. thickness at least 400 m.||||Overlies Hugh River Shale. Is overlain by Goyder Formation.||
16797|Shannon Formation|65489|5|Briefly described|p125|Cambrian|Cambrian|Amadeus Basin.||Unit in Pertaoorrta Group.||Is overlain by Goyder Formation.||
16797|Shannon Formation|67326|5|Briefly described|p2, p4|Late Cambrian|Middle Cambrian|Amadeus Basin.||Pertaoorrta Group.||Overlies Giles Creek Dolostone. Is overlain by Jay Creek Limestone and Goyder Formation. Equivalent to Petermann Sandstone.||
16797|Shannon Formation|67565|6|Mentioned|p40.|||Eastern Amadeus Basin. The lower part is correlated with Illara Sandstone in the Gardiner Range.||||||
16797|Shannon Formation|67856|6|Mentioned|p338 fig 4-30|Cambrian|Cambrian|||Of Pertaoorta Group.||||
16797|Shannon Formation|68323|6|Mentioned|p4 Fig.2|Late Cambrian|Middle Cambrian|Amadeus Basin.||Pertaoorrta Group.||||
16797|Shannon Formation|69437|5|Briefly described|p22:10|Series 3|Series 3|Amadeus Basin.||||Overlies Giles Creek Dolostone. Is overlain by Goyder Formation.||12-JUL-16
16797|Shannon Formation|69438|4|Described|p23:2-3, 8, 24-25, 28, 30-32, 43, 59|Late Cambrian|Middle Cambrian|Wells et al. (1967). Amadeus Basin. Over 700m thick, thinning to the N and W. Hydrocarbon source rock intervals may be present.||Pertaoorrta Group.||Para/disconformably overlies Giles Creek Dolostone. Is overlain conformably by Goyder Formation. Equivalent to Illara Sandstone and upper Hugh River Shale. Flanks the Jay Creek Limestone.|Lower part is 270m of silty shale with interbeds of thin siltstone and dolostone; upper part is ribboned carbonate and mudstone, grainstone and thrombolites, stromatolites and evaporites.|12-JUL-16
16797|Shannon Formation|69449|6|Mentioned|p34:2 Fig.34.2|Cambrian|Cambrian|Eastern Amadeus Basin.||||||12-JUL-16
16797|Shannon Formation|69673|5|Briefly described|p64 fig 53, p66, p80, p81, p102, p103|Cambrian|Cambrian|Potential source rock and potential for unconventional petroleum. Greater than 700m thick.||||Disconformably overlies Giles Creek Dolostone, conformably overlain by lower Goyder Formation, correlated with Arrinthrunga Formation|Silty shale with interbeds of thin siltstone and dolostone.|
16797|Shannon Formation|70752|5|Briefly described|p126 Fig.1|Cambrian|Cambrian|||Pertaoorrta Group.|||Siltstone and shale; fossiliferous and stromatolitic limestone and dolostone.|
16797|Shannon Formation|71114|4|Described|p171, p170 fig 1b, p172-4, p176-180|Guzhangian||Amadeus Basin. Deposited between ~511 and 490 Ma, in the intertidal to subtidal zone on a carbonate platform/shelf under intermittent evaporitic conditions. 391m thick in Dingo 1 well.||||Overlies Hugh River Shale. Is overlain by Goyder Formation or Jay Creek Limestone. Upper part equivalent to Jay Creek Limestone.|Characterised by oolitic, stromatolitic limestones. Lower part is dominated by silty shale with dolostone interbeds. Upper part transgresses into a carbonate-rich succession during sea level rise.|14-FEB-18
16797|Shannon Formation|71279|5|Briefly described|p355 Fig.2, p363, p382 Tb.1|Late Cambrian|Middle Cambrian|Amadeus Basin. Modelled magnetic properties.||Pertaoorrta Group.||||
16797|Shannon Formation|71800|6|Mentioned|p26 fig 3|Late Cambrian|Middle Cambrian|Amadeus Basin.||||Overlies the Giles Creek Dolomite. Overlain by the Goyder Formation.||
16797|Shannon Formation|72358|5|Briefly described|p117-119,121, 123, 126|Series 3|Series 3|Of Amadeus Basin. Deposited in the supratidal to subtidal zone on carbonate platform/shelf with intermittent evaporitic conditions (Kennard, 1994; Schmid, 2017). The upper section is sometimes (incorrectly?) referred to as Jay Creek Limestone, but referred to this study as Jay Creek Limestone equivalent. Contains evidence of microbial communities included Girvanella (calcareous green algae) at Ross River (Kennard, 1994).||||Overlain by the Goyder Formation. Correlable to Petermann Sandstone.|Oolitic and stromatolitic limestones.|10-JAN-20
16797|Shannon Formation|72489|5|Briefly described|p3, p4, p5, p7 Fig.6, p8, p9,p12|Late Cambrian|Late Cambrian|Located in the Amadeus Basin. Age bracketted between ca. 502 to 497 Ma through correlation.||||Upper part correlated with Jay Creek Limestone.|Stromatolitic  and oolitic limestones.|
16797|Shannon Formation|72516|6|Mentioned|p92, 93|Cambrian|Cambrian|Amadeus Basin.||||Equivalent to the Steamboat Sandstone. Upper part equivalent to Arrinthrunga Formation.||08-JUN-21
16797|Shannon Formation|72570|6|Mentioned|p8|Cambrian|Cambrian|Amadeus Basin.||||||
16797|Shannon Formation|73085|6|Mentioned|p1|late Cambrian|middle Cambrian|||Pertaoorrta Group [and equivalents?]||Underlain by Giles Creek Dolostone. Overlain by lower Goyder Formation. Partly equivalent to Jay Creek Limestone and Hugh River Shale.||
16826|Sherbrook Group|12781|5|Briefly described|p386, 391-392|Late Cretaceous|Late Cretaceous|Otway Basin. A very rapid increase in thickness occurs south of the Tartwaup Hingeline.|||Copa, Waarre, Paaratte, Flaxman Formations; Timboon Sandstone; Belfast Mudstone.|Overlies Otway Supergroup. Is overlain by Wangerrip Group.||
16826|Sherbrook Group|12796|5|Briefly described|p456 Fig. 2|||Geological Province: Otway Basin.||||||
16826|Sherbrook Group|22470|5|Briefly described|p13 Fig. 17|Maastrichtian|Turonian|Otway Basin.||||||
16826|Sherbrook Group|22674|5|Briefly described|p718, Fig.2 p719|Maastrichtian|Cenomanian|See also Fig.8 p725||||||
16826|Sherbrook Group|22875|3|Fully described|p37|Late Cretaceous|Late Cretaceous|~65-95Ma.||||||27-AUG-18
16826|Sherbrook Group|22914|6|Mentioned|17|||||||||
16826|Sherbrook Group|22944|6|Mentioned|p2||Cenomanian|||||||
16826|Sherbrook Group|23230|5|Briefly described|Table4-1p40, 40||Late Cretaceous|||||||
16826|Sherbrook Group|23792|5|Briefly described|p26|Maastrichtian|Turonian|Geological Province: Otway Basin.||||||21-OCT-08
16826|Sherbrook Group|23818|5|Briefly described|p162, 175|Late Cretaceous|Late Cretaceous|Of the Knight Group. Underlying unit: Otway Group. Overlying unit: Bahgallah Formation.||||||
16826|Sherbrook Group|23939|6|Mentioned|Fig.5|||May be Late Cretaceous in age.||||||
16826|Sherbrook Group|24056|4|Described|p85|Late Cretaceous|Late Cretaceous|Geological Basin: Otway Basin.||||||
16826|Sherbrook Group|24200|5|Briefly described|p408|Maastrichtian|Maastrichtian|Geological Province: Otway basin.  See also p423 Figs. 15 & 16, p 428 Fig. 18.  Sherbrook Group Equivalents discussed throughout text.||||||
16826|Sherbrook Group|24323|5|Briefly described|p136|Late Cretaceous|Late Cretaceous|Geological Province: Otway Basin. Overlain by the Wangerrip Group.||||||
16826|Sherbrook Group|24453|5|Briefly described|p809 Fig.2|Maastrichtian|Cenomian|Geological Province: Otway Basin.||||||07-FEB-11
16826|Sherbrook Group|24551|5|Briefly described|p240, Fig. 9.2|Late Cretaceous|Late Cretaceous|||||||
16826|Sherbrook Group|24562|4|Described|p6, 8, 37 Fig. 2|Late Cretaceous|Late Cretaceous|Maximum Thickness: 5000m+.  Includes: Waarre Sandstone, Flaxmans Formation, Belfast Mudstone, Nullawarre Greensand, Paaratte Formation, Timboon Sandstone.  Geological Province: Otway Basin.||||||
16826|Sherbrook Group|29697|6|Mentioned|Fig.11|||||||||
16826|Sherbrook Group|29856|5|Briefly described|p38|||||||||
16826|Sherbrook Group|30499|6|Mentioned|p92|||Stratigraphy||||||
16826|Sherbrook Group|30576|6|Mentioned|Fig.1|||||||||
16826|Sherbrook Group|30578|6|Mentioned|p6|||||||||
16826|Sherbrook Group|30905|6|Mentioned|p149|||||||||
16826|Sherbrook Group|30928|6|Mentioned|Map legend|Late Cretaceous|Late Cretaceous|||||||
16826|Sherbrook Group|31202|5|Briefly described|p218|||Unconformity with Otway Gp. & rift formation||||||
16826|Sherbrook Group|31372|6|Mentioned|p9|||||||||
16826|Sherbrook Group|31624|6|Mentioned|p98|||U.Cret. Contains Curdies Fm. & Paaratte Fm.||||||
16826|Sherbrook Group|31625|6|Mentioned|Fig. 5.2|||U.Cret.||||||
16826|Sherbrook Group|31920|3|Fully described|p50|||U.Cret. See also Fig.3-2||||||
16826|Sherbrook Group|31922|6|Mentioned|p187|||||||||
16826|Sherbrook Group|31923|6|Mentioned|p16|||||||||
16826|Sherbrook Group|32162|6|Mentioned|p58|||See also Fig. 5||||||
16826|Sherbrook Group|32344|6|Mentioned|Fig.2|||||||||
16826|Sherbrook Group|32852|6|Mentioned|P110|||||||||
16826|Sherbrook Group|32894|6|Mentioned|Table 2-1|||||||||
16826|Sherbrook Group|32897|4|Described|p177|||U.Cret.||||||
16826|Sherbrook Group|32898|6|Mentioned|Table 2-1|||||||||
16826|Sherbrook Group|33165|6|Mentioned|Chart|||Correlation chart only||||||
16826|Sherbrook Group|33320|5|Briefly described|p57|||Palynology & Strat.||||||
16826|Sherbrook Group|33940|6|Mentioned|p393|||U.Cret.||||||
16826|Sherbrook Group|34063|6|Mentioned|p3|||Table. U.Cret.||||||
16826|Sherbrook Group|34308|6|Mentioned|p175|||U.Cret.||||||
16826|Sherbrook Group|34611|6|Mentioned|p162|||Marine||||||
16826|Sherbrook Group|34987|5|Briefly described|p170|||||||||
16826|Sherbrook Group|35013|6|Mentioned|p393|||||||||
16826|Sherbrook Group|35066|6|Mentioned|p201|||||||||
16826|Sherbrook Group|35285|5|Briefly described|p414|||||||||
16826|Sherbrook Group|36913|6|Mentioned|Fig.4|||||||||
16826|Sherbrook Group|37065|6|Mentioned|p42|||||||||
16826|Sherbrook Group|37783|6|Mentioned|Fig.10|||||||||
16826|Sherbrook Group|38221|6|Mentioned|Fig.4|||Otway Basin||||||
16826|Sherbrook Group|38625|6|Mentioned|p271|||||||||
16826|Sherbrook Group|38717|5|Briefly described|p20|||||||||
16826|Sherbrook Group|39077|6|Mentioned|Table 2|||||||||
16826|Sherbrook Group|39211|6|Mentioned|Fig.45|||||||||
16826|Sherbrook Group|39315|6|Mentioned|Fig.7|||||||||
16826|Sherbrook Group|40003|5|Briefly described|p43|||See also Fig.10||||||
16826|Sherbrook Group|40560|6|Mentioned|p4|||||||||
16826|Sherbrook Group|40947|6|Mentioned|p3|||||||||
16826|Sherbrook Group|41016|5|Briefly described|Mention|||||||||
16826|Sherbrook Group|41171|6|Mentioned|p168|||||||||
16826|Sherbrook Group|41185|5|Briefly described|p175|||See also Fig.7a||||||
16826|Sherbrook Group|41269|5|Briefly described|p245|||||||||
16826|Sherbrook Group|41318|6|Mentioned|p191|||||||||
16826|Sherbrook Group|41487|5|Briefly described|p625|||||||||
16826|Sherbrook Group|41552|6|Mentioned|p459|||||||||
16826|Sherbrook Group|41642|6|Mentioned|p219|||||||||
16826|Sherbrook Group|41701|6|Mentioned|Map legend|late Campanian||||||||
16826|Sherbrook Group|41704|6|Mentioned|p100|||||||||
16826|Sherbrook Group|41706|5|Briefly described|p145|||||||||
16826|Sherbrook Group|41714|6|Mentioned|p301|||||||||
16826|Sherbrook Group|41726|5|Briefly described|p420|||||||||
16826|Sherbrook Group|41769|5|Briefly described|p12|||||||||
16826|Sherbrook Group|41797|5|Briefly described|p224|||||||||
16826|Sherbrook Group|41868|4|Described|p533|||||||||
16826|Sherbrook Group|41936|6|Mentioned|p75|||||||||
16826|Sherbrook Group|42075|5|Briefly described|Fig.13 P252|||||||||
16826|Sherbrook Group|42079|6|Mentioned|Fig.10 P272|||||||||
16826|Sherbrook Group|42152|6|Mentioned|p15|||||||||
16826|Sherbrook Group|42184|6|Mentioned|Fig.2 P348|||||||||
16826|Sherbrook Group|42318|6|Mentioned|p7|||||||||
16826|Sherbrook Group|42361|4|Described|p12, p18|||||||||
16826|Sherbrook Group|42524|5|Briefly described|Fig.3 P27|||||||||
16826|Sherbrook Group|42545|6|Mentioned|p4|||Otway Basin||||||
16826|Sherbrook Group|42555|5|Briefly described|284|||||||||
16826|Sherbrook Group|42599|5|Briefly described|Fig.3 P614|||||||||
16826|Sherbrook Group|42827|3|Fully described|p243|||see also Table 7.12||||||
16826|Sherbrook Group|42863|5|Briefly described|Fig.14|||Variation on Victorian unit.||||||
16826|Sherbrook Group|43052|5|Briefly described|Fig.2.16|||||||||
16826|Sherbrook Group|43171|4|Described|2-8|Maastrichtian|Cenomanian|Of Otway Supergroup.||||||21-OCT-08
16826|Sherbrook Group|43195|5|Briefly described|Map Legend||Late Cretaceous|See also commentary on back of map.||||||
16826|Sherbrook Group|43208|5|Briefly described|map legend|Maastrichtian|Cenomanian|||||||
16826|Sherbrook Group|43219|5|Briefly described|Fig.3,p6.|Maastrichtian|Cenomanian|||||||
16826|Sherbrook Group|43590|4|Described|p12||Late Cretaceous|||||||
16826|Sherbrook Group|43660|6|Mentioned|Fig.6,p15||Late Cretaceous|||||||
16826|Sherbrook Group|43733|5|Briefly described|p9||Late Cretaceous|||||||
16826|Sherbrook Group|43744|6|Mentioned|Fig.3,p3|||||||||
16826|Sherbrook Group|43747|6|Mentioned|p5||Cenomanian|||||||
16826|Sherbrook Group|43783|6|Mentioned|Fig14, p11||Late Cretaceous|||||||
16826|Sherbrook Group|43784|4|Described|Fig10, p12, p29||Late Cretaceous|||||||
16826|Sherbrook Group|43814|6|Mentioned|Fig.3,p115|||||||||
16826|Sherbrook Group|43937|5|Briefly described|Map Legend|Santonian|Aptian|||||||
16826|Sherbrook Group|44133|5|Briefly described|p142, 94 Fig. 9.2, 146|Mesozoic|Cretaceous|Geological Province: Otway Basin.||||||
16826|Sherbrook Group|44135|6|Mentioned|p49|||Geological province: Otway Basin. Mentioned in the context of correlates.||||||07-DEC-09
16826|Sherbrook Group|46802|6|Mentioned|Table 1|||||||||
16826|Sherbrook Group|46970|6|Mentioned|Fig.17|||||||||
16826|Sherbrook Group|48911|4|Described|p17|||Cret. Formations in group||||||
16826|Sherbrook Group|48977|5|Briefly described|p26|||See also p2 & Fig.5. Upper Cret.||||||27-AUG-18
16826|Sherbrook Group|49060|6|Mentioned|Fig.32|||||||||
16826|Sherbrook Group|60451|5|Briefly described|p95 Fig. 61|||||||||
16826|Sherbrook Group|60538|5|Briefly described|p474 Fig. 13|||Geological Province: Otway Basin.||||||
16826|Sherbrook Group|61017|5|Briefly described|p5|Maastrichtian|Turonian|Geological Province: Otway Basin.||||||07-FEB-11
16826|Sherbrook Group|61045|6|Mentioned|p93|Late Cretaceous|Late Cretaceous|||||||
16826|Sherbrook Group|61155|5|Briefly described|p18|||Includes the Timboon Sand Member. Unconformably overlain in part by Pebble Point Formation. Age is pre-Cainozoic. Geological Province: Otway Basin.||||||
16826|Sherbrook Group|61182|3|Fully described|p14, p35|Late Cretaceous|Late Cretaceous|Comprises Waarre and Flaxman Fms, Belfast Mudstone, Nullawarre Greensand and Paarratte Fm. Unconformable over Otway Group; unconformable beneath Wangerrip Gp. Max. thickness: 1790m. Age: 97-65Ma. Geol.Prov:Otway Basin. Included by some in Wangerrip Group.||||||
16826|Sherbrook Group|61230|5|Briefly described|p319, p329, p333, p337, p344.     |Late Cretaceous|Late Cretaceous|Of the Otway Delta. Hosts gas reserves. Deposition occurred in a variety of environments, from flood plain to upper slope.|||Includes Waarre, Flaxman, Belfast Mudstone and Paaratte Formations; Nullawarre Greensand; Skull Creek Mudstone and Timboon Sandstone.|||
16826|Sherbrook Group|61470|5|Briefly described|p28 Fig. 5|Maastrichtian|Turonian|Includes Flaxman Fm., Belfast Mudstone, Nullawarre Greensand, Skull Creek Mudstone, Paaratte Fm., Timboon Sandstone and Massacre Shale. Geological Province: Otway Basin.||||||12-OCT-05
16826|Sherbrook Group|61547|5|Briefly described|p461 Fig.2, p462. |Late Cretaceous|Late Cretaceous|Fluvio-deltaic deposition.|||Includes Timboon Sandstone, Paaratte Formation, Belfast Mudstone, Flaxman Formation and Shipwreck Subgroup.|Overlies Otway Supergroup. Is unconformably overlain by Wangerrip Group.|Frequent mudstone and massive sandstone units.|
16826|Sherbrook Group|61607|6|Mentioned|p5 Fig. 2|Late Cretaceous|Late Cretaceous|Geological Province: Otway Basin.||||||12-MAR-09
16826|Sherbrook Group|61608|6|Mentioned|p41 Fig. 5|||Refers to equivalent unit.||||||
16826|Sherbrook Group|61622|5|Briefly described|p436 Fig. 2, p438 Fig. 4|Cretaceous|Cretaceous|Includes; Copa, Flaxman and Paaratte Formations, Timboon and Waarre Sandstone and Belfast Mudstone. Geological Province: Otway Basin.||||||07-FEB-11
16826|Sherbrook Group|61623|5|Briefly described|p447, p452, p449 Fig. 4|Late Cretaceous|Late Cretaceous|Includes; Flaxman, Waarre and Paaratte Formations, Timboon Sandstone and Belfast Mudstone.Geological Province: Otway Basin.||||||
16826|Sherbrook Group|61624|6|Mentioned|p465|Cretaceous|Cretaceous|Geological Province: Otway Basin.||||||07-APR-09
16826|Sherbrook Group|61625|5|Briefly described|p475|Late Creatceous|Late Cretaceous|Includes Waarre Formation, Belfast Mudstone, Nullawarre Greensand, Paaratte Formation, Flaxman Formaion and Timboon Sandstone. Geological Province: Otway Basin.||||||07-FEB-11
16826|Sherbrook Group|61626|5|Briefly described|p486, p486 Fig. 2, p488 Fig. 4, p488|Late Cretaceous|Late Cretaceous|Includes; Waarre, Flaxman and Paaratte Formations, Belfast Mudstone and Timboon Sandstone. Geological Province: Otway Basin.||||||
16826|Sherbrook Group|61627|5|Briefly described|p499, p500 Fig. 2|Late Cretaceous|Late Cretaceous|Includes Shipwreck Subgroup. Includes Paaratte Formation and Timboon Sandstone. Geological Province: Otway Basin.||||||07-FEB-11
16826|Sherbrook Group|61628|5|Briefly described|p507, p509 Fig. 3, p511, p512, p515|Late Cretaceous|Late Cretaceous|Includes; Waarre, flaxman and Paaratte Formations, Belfast Mudstone, Nullawarre Greensand and Timboon Sandstone. Geological Province: Otway Basin.||||||
16826|Sherbrook Group|62896|6|Mentioned|p88|Mesozoic|Mesozoic|||||||07-FEB-11
16826|Sherbrook Group|63122|5|Briefly described|p17 Fig. 4.3, p21, p41|Maastrichtian|Cenomanian|Includes the Copa, Flaxman and Paaratte Formations, Waarre and Timboon Sandstones and Belfast Mudstone. Geological Province: Otway Basin.||||||
16826|Sherbrook Group|63124|3|Fully described|p47, p49 Fig. 5.2, p74-77|Late Cretaceous|Late Cretaceous|Includes Shipwreck Subgroup and Copa, Flaxman and Paaratte Formations, Waarre and Timboon Sandstones and Belfast Mudstone. Unconformable over Eumeralla Formation. Max. age: 97Ma. Max. thickness: 5000m. Geological Province: Otway Basin.||||||31-JAN-08
16826|Sherbrook Group|63125|5|Briefly described|p111|Early Paleocene|Late Cretaceous|Min. age: ~65Ma. Geological Province: Otway Basin||||||
16826|Sherbrook Group|63129|6|Mentioned|p137|||Geological Province: Otway Basin.||||||30-JAN-08
16826|Sherbrook Group|63130|5|Briefly described|p143|||Geological Province: Otway Basin. North of Tartwaup Hingeline this is a thin, condensed sandy sequence with poor hydrocarbon trapping potential.||||||
16826|Sherbrook Group|63150|5|Briefly described|p96|Late Cretaceous|Late Cretaceous|Geological province: Otway Basin. Plant microfossils are abundant and diverse in claystone sections of this group and are only absent from sandstone lithologies.||||||
16826|Sherbrook Group|63173|5|Briefly described|p342 Fig. 9.2|Late Cretaceous|Late Cretaceous|Geological Province: Otway Basin, offshore.||||||07-FEB-11
16826|Sherbrook Group|63269|5|Briefly described|p603-605, p607, p609|Late Cretaceous|Late Cretaceous|Otway Basin. A thick, syn-rift siliciclastic succession.|||Waarre, Flaxman, Paaratte Formations; Belfast Mudstone; Nullawarre Greensand; Timboon Sandstone.|Unconformably overlies Otway Group. Is overlain unconformably by Wangerrip Group.||
16826|Sherbrook Group|63431|5|Briefly described|p677 Fig. 2|Maastrictian|Cenomanian|Includes the Shipwreck Subgroup, Flaxman Formation and Belfast Mudstone, Paaratte Formation and Timboon Sandstone. Overlain by Wangerrip Group. Geological Province: Penola Trough/Otway Basin.See also p680.||||||07-FEB-11
16826|Sherbrook Group|63740|6|Mentioned|p88|Mesozoic|Mesozoic|||||||07-FEB-11
16826|Sherbrook Group|64314|5|Briefly described|p504|Late Cretaceous|Late Cretaceous|Unconformably overlain by Wangerrip Group.||||||21-OCT-08
16826|Sherbrook Group|66245|5|Briefly described|p5, p6 Fig.5, p15, p30. |Late Cretaceous|Late Cretaceous|The authors call for subdivision of this unit; they split it into six depositional sequences. Deposited as the Otway Basin continued to widen. Provided necessary overburden to mature source intervals near the base of the Eumeralla Formation.|||Includes Waarre, Flaxman and Paaratte Formations, Belfast Mudstone, Nullawarre Greensand and Timboon Sandstone.|||
16826|Sherbrook Group|67061|5|Briefly described|p545, p546 Fig.3.|Maastrichtian|Turonian|Otway Basin. Equivalent to lower parts of Eastern View Group (Torquay Sub-basin).|||Includes Copa, Waarre, Flaxman and Paaratte Formations; Belfast and Skull Creek Mudstones; and Nullawarre Greensand.|||
16826|Sherbrook Group|67366|5|Briefly described|p101. |Late Cretaceous|Late Cretaceous|The primary reservoir unit in onshore gas fields of northeast Otway Basin.|||Includes Waarre, Flaxman, Belfast, Nullawarre and Paaratte Formations, Skull Creek Mudstone and Timboon Sandstone.|Unconformably overlies Otway Group. Is overlain unconformably by Wangerrip Group.||
16826|Sherbrook Group|67367|5|Briefly described|p130, p131 Fig.2, p133. |Late Cretaceous|Late Cretaceous|Non-marine to marine siliciclastics. Stratigraphic equivalent to Latrobe Group, offshore Gippsland Basin. Overall, the hydrocarbon source rock quality of this Group is fairly poor.|||Includes Waarre, Flaxman and Paaratte Formations, Belfast and Skull Creek Mudstones, Nullawarre Greensand, Timboon Sandstone and Wiridjil Gravels.|||
16826|Sherbrook Group|67541|6|Mentioned|p76 Fig.1|||||||||
16826|Sherbrook Group|69297|6|Mentioned|p79, p84, p98, p112, p116, p117|Maastrichtian|Cenomanian|Otway Basin. Is the primary reservoir facies in the offshore Otway Basin.|||Includes the Copa Formation, Waarre Formation, Flaxman Formation, Belfast Mudstone, Paaratte Formation and the Timboon Sandstone.|Unconformably overlies the Otway Group. Overlain by the Wangerrip Group.||
16826|Sherbrook Group|69651|5|Briefly described|p6, p10, p12, p26, p31-34, p38|Late Cretaceous|Late Cretaceous|Otway and Sorell Basins. Up to 5km of coastal plain, deltaic and inner shelf sediments. Minor amounts of free oil recorded in Cape Sorell 1 is evidence for an active Cretaceous petroleum system in the Strahan Sub-basin. Contains the primary reservoir facies in offshore Otway Basin. Modelling diagrams.|||Waarre, Flaxman, Paaratte Formations; Belfast Mudstone, Nullawarre Greensand, Timboon Sandstone.|Unconformably overlies Otway Group. Is overlain unconformably by Wangerrip Group.|Interbedded conglomeratic sandstone, sandstone, siltstone and claystone; the latter two dominating at depth.|17-JUN-20
16826|Sherbrook Group|69879|5|Briefly described|p418, p424|Maastrichtian|Maastrichtian|Strahan Sub-basin. Shown as Sherbrook Group equivalent. Offshore exploration well Cape Sorell 1.||||Underlies Wangerrip Group.|Quartzitic sandstone with basal conglomerate. Oil show. Mainly sandstone and shale with some coaly beds deposited in a paralic to coastal plain environment.|
16826|Sherbrook Group|70077|5|Briefly described|Nelson:Fig.2; p2.Regional:Fig.4;p7-8,p10|Late Cretaceous|Late Cretaceous|Otway Basin: Gambier Embayment and Voluta Trough. Distal equivalents in the Nelson Sub-basin may be petroleum sources of the Austral 3 Petroleum System.|||Copa, Waarre, Flaxman, Mount Salt, Paaratte Formations; Skull Creek and Belfast Mudstones; Nullawarre Greensand and Timboon Sandstone.|Overlies Otway Group. Is overlain by Wangerrip Group.||
16826|Sherbrook Group|70078|5|Briefly described|Northern: Fig.2; p2. Regional: Fig.4; p6|Late Cretaceous|Late Cretaceous|Gambier Embayment and Voluta Trough. Fluvio-deltaic to marine sediments equivalent to this unit in the Sorell Basin are potential oil and gas sources in the Basin. Contains potential structural traps (high-side fault traps and faulted anticlines).|||Copa, Waarre, Flaxman, Mount Salt, Paaratte Formations; Belfast Mudstone; Timboon Sandstone.|Overlies Otway Group. Is overlain by Wangerrip Group.||
16826|Sherbrook Group|70379|6|Mentioned|p723-727, p732|||Otway Basin.||||Overlies Eumeralla Formation. Is overlain by Wangerrip Group.||
16826|Sherbrook Group|71593|5|Briefly described|p51|Eocene|Cretaceous|||||||
16826|Sherbrook Group|72050|6|Mentioned|p237, 240 Fig.9, 242 Fig.13|Maastrichtian|Cenomanian|||||||
16826|Sherbrook Group|73356|6|Mentioned|p2, p15-16||||||||Fluvial, deltaic and shallow marine sediments.|
16826|Sherbrook Group|73357|6|Mentioned|p43, p45, p47|Maastrichtian|Turonian|Otway Basin.||||||
16826|Sherbrook Group|73383|4|Described|p2-4, p7 Tb.3.1, p10, p21, p27, p214|Maastrichtian|Cenomanian|Otway Basin. Equivalent to chemostratigraphic Sequence S5 containing generally lower Ti/Th values than other sequences in Otway Basin. Contains several occurrences of high Fe and P intervals, likely related to berthierine 'greensands'. See also p83.|||Waarre Formation, Flaxman Formation, Belfast Mudstone, Nullawarre Greensand, Skull Creek Mudstone, Paaratte Formation, Timboon Sandstone|Overlies Otway Group, Eumeralla Formation, underlies Wangerrip Group|Contains clastic units of sandstones, mudstones, siltstones and marine shales. Includes sandstone, quartz arenite based on geochemistry.|
16826|Sherbrook Group|73385|5|Briefly described|p3-6, p19, p20 Fig.5.4, p21-24|Maastrichtian|Cenomanian|Otway Basin. Deposited in a series of half-grabens and embayments. Sedimentary package of the Sherbrook group is much thinner in the Tyrendarra Embayment than in the Port Campbell Embayment. Sedimentary package thins significantly across the Mussel Platform, Prawn Platform and Bridgewater High, and thickens in the Shipwreck Trough.|||Waarre Formation, Flaxman Formation, Belfast Mudstone, Nullawarre Greensand, Skull Creek Mudstone, Paaratte Formation, Timboon Sandstone|Overlies Otway Group, Eumeralla Formation, underlies Wangerrip Group, Pebble Point Formation.|Sequence of fluvial, deltaic and shallow marine sediments.|
16826|Sherbrook Group|73386|4|Described|p1-2, p4-7, p10-12, iii, Attachment A1|Maastrichtian|Turonian|Otway Basin. Absent from northern margin of the basin, increases in thickness towards the south. Represents a shift from fluvial to marginal marine and lower coastal plain sandstones, mudstones and coals, deposited due to renewed extension. Contact with Otway Group is conformable or mildly disconformable in Late Cretaceous depocentres, unconformable where the Sherbrook Group wedges out against inversion structures. Top of the group is a major flooding surface, upper boundary marked by regional intra-Maastrichtian unconformity. Contains Phyllocladidites mawsonii to Lower Forcipites longes spore-pollen zones, and chemostratigraphic sequence S5 of Forbes et al. (2020).|||Timboon Sandstone, Paaratte Formation, Skull Creek Mudstone, Nullawarre Greensand, Belfast Mudstone, Flaxman Formation, Waarre Formation|Overlies Otway Group, Eumeralla Formation, unconformably underlies Wangerrip Group|Sandstones, mudstones and coals.|
16826|Sherbrook Group|73594|5|Briefly described|p2-5|Maastrichtian|Cenomanian|Otway Basin. Sedimentary fill of second phase of rifting. Reflects increasing marine influence. Angular unconformity with Eumeralla Formation in places of Cenomanian uplift such as the Otway Ranges.|||Waarre Formation, Flaxman Formation, Belfast Mudstone, Nullawarre Greensand, Skull Creek Mudstone, Paaratte Formation, Timboon Sandstone|Conformably overlies Eumeralla Formation, Otway Group. Underlies Wangerrip Group.|Includes a basal transgressive sequence of sandstones, mudstones and coals, overlain by silty mudstones and glauconitic sandstones.|
16914|Simmens Quartzite Member|24321|5|Briefly described|Map legend|Late Adelaidean|Late Adelaidean|Parent: Tent Hill Formation||||||
16914|Simmens Quartzite Member|30801|6|Mentioned|p5|||Tent Hill Formation. Table P5-6||||||
16914|Simmens Quartzite Member|30807|6|Mentioned|p102|||Suggested map symbol||||||
16914|Simmens Quartzite Member|31395|6|Mentioned|p64|||||||||
16914|Simmens Quartzite Member|31540|6|Mentioned|p10|||Equiv. Arcoona Qzte. Mb.||||||
16914|Simmens Quartzite Member|33474|6|Mentioned|Fig.3|||||||||
16914|Simmens Quartzite Member|34536|6|Mentioned|Map legend|Adelaidean|Adelaidean|Marinoan||||||
16914|Simmens Quartzite Member|39808|6|Mentioned|p223|||||||||
16914|Simmens Quartzite Member|40448|5|Briefly described|p38|||||||||
16914|Simmens Quartzite Member|41429|6|Mentioned|p228|||||||||
16914|Simmens Quartzite Member|42222|6|Mentioned|p19|||||||||
16914|Simmens Quartzite Member|42469|4|Described|p25|||||||||
16914|Simmens Quartzite Member|42600|6|Mentioned|p9|||||||||
16914|Simmens Quartzite Member|42721|5|Briefly described|map legend|Marinoan||||||||
16914|Simmens Quartzite Member|43052|5|Briefly described|p192,table 6.1|||of Tent Hill Formation||||||
16914|Simmens Quartzite Member|43094|4|Described|Table 5|||of Tent Hill Formation||||||
16914|Simmens Quartzite Member|44660|14|Not recorded|map legend|||Marinoan.||||||
16914|Simmens Quartzite Member|60953|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Deltaic sandstone.||||||
16914|Simmens Quartzite Member|60955|5|Briefly described|Map Legend|||Equivalent to Arcoona Quartzite Member.||||||
16914|Simmens Quartzite Member|61108|5|Briefly described|map legend|Adelaidean|Adelaidean|Deltaic sandstone.||||||
16914|Simmens Quartzite Member|65376|6|Mentioned|p140 Fig.4.22.|Neoproterozoic|Neoproterozoic|||||||
16914|Simmens Quartzite Member|68131|6|Mentioned|p89|Neoproterozoic|Neoproterozoic|||||||
16914|Simmens Quartzite Member|69666|6|Mentioned|p27 Fig.3|Neoproterozoic|Neoproterozoic|||||||
16914|Simmens Quartzite Member|70333|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Parent Formation not named.|||||Quartzite, blocky; sandstone, cream-coloured.|
16914|Simmens Quartzite Member|70334|5|Briefly described|p40,57-58,66-68,72,77,88,92|Ediacaran|Ediacaran|Geological province: Gawler Craton. Of Stuart Shelf. Also referred to as Simmens Quartzite in text. Shoreline marine facies (Dyson, 1996b). Clean sands deposited as a continuous sheet over the Stuart Shelf and Adelaide Geosyncline. Poorly exposed on the Siemens Plateau (weathered and blacketed by transported Quaternary cover).||Unit of Tent Hill Formation.|||Blocky white quartzite and cream sandstone.|
16914|Simmens Quartzite Member|70406|5|Briefly described|p117, 121|||Formerly of Tent Hill Formation. Elevated herein to formation status.||||||
16914|Simmens Quartzite 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 Corraberra Sandstone Member.|Grey to reddish brown massive to cross-bedded quartzite; with silcrete skins.|
16914|Simmens Quartzite Member|71129|4|Described|p128,131,133-134,137-138|Ediacaran|Ediacaran|Of Stuart Shelf. Thickness: up to 10m. Deposited as progradational ebb-flow tidal sand sheets in a tidal-dominated shoreface environment above fairweather wave base. Forms a resistent cap, and is poorly exposed at the top of Simmens Plateau. Whereelse preserved, forms prominent plateaus and mesas. Experienced dissection and subsequent erosion of underlying strata and resulting in formation of scarps. At a later time, experienced landslides in warmer and wetter climates, producing landslides and debris flow deposits. See also p141,145-148,164,209-210,225,229.||Unit of Tent Hill Formation.||Uppermost unit of Tent Hill Formation. Overlain unconformably by Sugarloaf Dam Sandstone. Underlain by Corroberra Sandstone Member. Partially equivalent to ABC Range Quartzite.|Blocky white to greyish-white thin- to very thick-bedded fine- to medium-grained quartz arenites.|13-NOV-19
16914|Simmens Quartzite Member|71131|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Age shown as Marinoan. Source of clasts in unconsolidated pebbly and sandy regolith.||Tent Hill Formation.|||Grey to reddish-brown, massive to cross-bedded quartzite; with silcrete skins.|
16914|Simmens Quartzite Member|71895|5|Briefly described|p10, APP4. p4, |||Stuart Shelf.||Wilpena Group||||
16914|Simmens Quartzite Member|72247|5|Briefly described|p43|Neoproterozoic|Neoproterozoic|Of Adelaide Geosyncline.||Unit of Wilpena Group.||Equivalent to Arcoona Quartzite. Underlain by Corraberra Sandstone Member.||
16914|Simmens Quartzite Member|73103|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic||||||Quartzite, blocky; sandstone, cream coloured.|
16914|Simmens Quartzite Member|73110|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic||||||Quartzite, blocky; sandstone, cream coloured.|
16914|Simmens Quartzite Member|73227|5|Briefly described|p25|||Torrens Hinge Zone.||Tent Hill Formation, Wilpena Group||Underlain by Corraberra Sandstone Member. Equivalent to 'Arcoona Quartzite'|Cream to red silicified quartz sandstone.|
16914|Simmens Quartzite Member|73234|6|Mentioned|p6-7, p9, p12-14, p20|||Deposited in high energy marine environments in shallow waters. Youngest preserved sedimentary rock of the Adelaidean system in the Six Mile Hill area. Affected by paleolandslides.||Tent Hill Formation, Wilpena Group||||
16923|Simpson Sand|23154|5|Briefly described|Map Legend|Holocene|Holocene|Geological Province - Lake Eyre Basin - Callabonna Basin.||||||
16923|Simpson Sand|23478|5|Briefly described|p28|Holocene|Pleistocene|||||||
16923|Simpson Sand|24104|6|Mentioned|p149|||Geological Province: Otway Basin.||||||
16923|Simpson Sand|24321|5|Briefly described|Map legend|Late Pleistocene|Pleistocene|||||||
16923|Simpson Sand|30056|6|Mentioned|Table 4|||||||||
16923|Simpson Sand|30749|2|Defined|p1|Recent|late Pleistocene|Late Pleistocene-Recent||||||
16923|Simpson Sand|30804|5|Briefly described|p14|||See also Table 1||||||
16923|Simpson Sand|30807|6|Mentioned|p101|||Suggested map symbol||||||
16923|Simpson Sand|30919|6|Mentioned|Map legend|Quaternary|Quaternary|||||||
16923|Simpson Sand|33827|6|Mentioned|p15|||||||||
16923|Simpson Sand|33828|6|Mentioned|Table 1|||||||||
16923|Simpson Sand|38068|6|Mentioned|p78|||||||||
16923|Simpson Sand|40910|6|Mentioned|p20|||||||||
16923|Simpson Sand|40911|6|Mentioned|Map legend|late Pleistocene|late Pleistocene|||||||
16923|Simpson Sand|40925|6|Mentioned|Map legend|Cenozoic|Cenozoic|||||||19-NOV-08
16923|Simpson Sand|40926|3|Fully described|p30|||||||||
16923|Simpson Sand|42746|5|Briefly described|Fig.2 P4|||||||||
16923|Simpson Sand|43053|5|Briefly described|Map Legend|Quaternary|Quaternary|||||||25-MAY-05
16923|Simpson Sand|43258|5|Briefly described|Map Legend|Holocene|Pleistocene|||||||
16923|Simpson Sand|43298|6|Mentioned|Map Legend|Holocene|Pleistocene|||||||
16923|Simpson Sand|44133|5|Briefly described|p247, 244 Table 11.3|Holocene|Pleistocene|Maximum Thiockness: 50m.||||||
16923|Simpson Sand|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
16923|Simpson Sand|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.||||||
16923|Simpson Sand|66131|6|Mentioned|p240|Holocene|Pleistocene|Simpson Desert. Called Coonarbine Formation in Strzelecki Desert.||||Equivalent to Coonarbine Formation.||
16923|Simpson Sand|68068|5|Briefly described|Map legend|Pleistocene|Pleistocene|Callabonna Sub-basin, Lake Eyre Basin. Marginal to windward side of pans and water courses; grades into lunettes (leeside transverse dunes) and other dunes.||||Interdigitates with Coonarbine Formation.|Hummocky, pale yellow, very fine- to medium-grained quartz sand; includes some local slopewash deposits from dune flanks.|
16923|Simpson Sand|69019|5|Briefly described|p124.|Holocene|Pleistocene|Of Firman (1970). Extensive dune fields, mapped as two units: longitudinal single and multicrested seif dunes, and hummocky dunes marginal to the windward side of pans. Rarely intertongues with Coonarbine Formation. Sometimes merges with lunettes. Age-dating discussed.|||||Loose quartz sand, very fine- to medium-grained.|
16923|Simpson Sand|69023|5|Briefly described|p132, p138-140|Holocene|Pleistocene|Of Firman (1970). Extensive dune fields spreading from Simpson Desert out into NT, Qld and NSW. Following use by Calley et al. (1994), mapped as two units: longitudinal single and multicrested dunes, and hummocky dunes marginal to the windward side of pans and to the W of Strzelecki Creek. Age discussed.|||||Loose quartz sand, commonly in three layers: reddish-yellow on top, reddish-yellow to yellowish-red in the middle, and a pale yellowish or reddish-brown basal layer.|
16923|Simpson Sand|70336|5|Briefly described|Map legend|Holocene|Pleistocene||||||Quartz sand, dune sand, aeolian, clay pans.|
16923|Simpson Sand|70338|5|Briefly described|Map legend.|Holocene|Pleistocene||||||Quartz sand, dune sand, aeolian, clay pans.|
16923|Simpson Sand|71321|6|Mentioned|p29|Quaternary|Quaternary|Of Simpson Desert.||||||
16987|Slapes Gully Member|22889|6|Mentioned|Table 1 on p32|Adelaidean|Adelaidean|Parent - Stonyfell Quartzite of the Bungarider Subgroup.||||||
16987|Slapes Gully Member|36835|6|Mentioned|p31|||||||||
16987|Slapes Gully Member|41404|6|Mentioned|p107|||See also Fig.23||||||
16987|Slapes Gully Member|43052|5|Briefly described|p181,Table 6.1|||of Stonyfell Quartzite||||||
16987|Slapes Gully Member|73188|6|Mentioned|p328|Neoproterozoic|Neoproterozoic|||Stonyfell Quartzite, Bungarider Subgroup, Burra Group||Underlain by Wattle Park Member.|Impure sandstones.|
17007|Smith Bay Shale|22458|6|Mentioned|p527||Cambrian|||||||
17007|Smith Bay Shale|22581|4|Described|Fig.2,p37|||Of the Kangaroo Island Group. Thickness: 200 m. Overlies Stokes Bay Sandstone. Overlain by White Point Conglomerate||||||02-JUL-08
17007|Smith Bay Shale|22766|4|Described|Fig.2 p561, 563|Early Cambrian|Early Cambrian|||||||
17007|Smith Bay Shale|22857|5|Briefly described|p88 Fig. 14.7A|Early Cambrian|Early Cambrian|Of the Kangaroo Island Group. Geological Province: Stansbury Basin.||||||
17007|Smith Bay Shale|22858|6|Mentioned|Fig14.7ap88-9|Toyonian|Toyonian|||||||
17007|Smith Bay Shale|23818|5|Briefly described|p87 Fig.33|Cambrian|Cambrian|Of the Kangaroo Island Group.||||||
17007|Smith Bay Shale|30982|6|Mentioned|p435|||||||||
17007|Smith Bay Shale|33332|6|Mentioned|p11|||L. Camb.||||||
17007|Smith Bay Shale|33471|6|Mentioned|Fig.1|||||||||
17007|Smith Bay Shale|34612|5|Briefly described|p105|||Cambrian. See Fig.33.||||||
17007|Smith Bay Shale|35255|6|Mentioned|Fig.8|||||||||
17007|Smith Bay Shale|36198|6|Mentioned|Fig.I.2|||||||||
17007|Smith Bay Shale|38873|4|Described|Table 3|||See also Fig.8||||||
17007|Smith Bay Shale|39842|6|Mentioned|p8|||||||||
17007|Smith Bay Shale|40856|6|Mentioned|Fig.23.6|||||||||
17007|Smith Bay Shale|41947|6|Mentioned|Fig.2 P17|||||||||
17007|Smith Bay Shale|42225|6|Mentioned|Fig.4 P224|||||||||
17007|Smith Bay Shale|42269|6|Mentioned|p341|||||||||
17007|Smith Bay Shale|42272|6|Mentioned|p413|||||||||
17007|Smith Bay Shale|44133|5|Briefly described|p4 Fig. 7.2, 12|Early Cambrian|Early Cambrian|Geological Province: Stansbury Basin. Overlies transitionally: Stokes Bay Sandstone.||||||
17007|Smith Bay Shale|62785|6|Mentioned|p44 Fig.1|Early Cambrian|Early Cambrian|North coast Kangaroo Island. Overlies Stokes Bay Sandstone and underlies White Point Conglomerate.||||||
17007|Smith Bay Shale|64282|5|Briefly described|Map legend|Early Cambrian|Early Cambrian|Of Kangaroo Island Group. Micaceous mudstone; siltstone; sandstone: an upper sandstone facies (pink, massive and laminated) and lower sandstone facies (grey-green/chocolate-brown, micaceous mudstone + siltstone).  Further lith.+ fossil details included.||||||02-JUL-08
17007|Smith Bay Shale|65375|5|Briefly described|p33.|Early Cambrian|Early Cambrian|||Unit in Kangaroo Island Group.||Overlies Stokes Bay Sandstone. Is overlain by White Point Conglomerate.||
17007|Smith Bay Shale|65667|6|Mentioned|p1222 Fig.1|Early Cambrian|Early Cambrian|Shown as older than White Point Conglomerate.||||||27-MAR-12
17007|Smith Bay Shale|65686|6|Mentioned|p411|Cambrian|Cambrian|Kangaroo Island||||||
17007|Smith Bay Shale|65892|5|Briefly described|p9 Fig.4, p22 Fig.10. |Early Cambrian|Early Cambrian|North Coast of Kangaroo Island.||||Overlies Stokes Bay Sandstone. Is overlain by White Point Conglomerate.||
17007|Smith Bay Shale|65921|6|Mentioned|p1, p2 (map legend).|Cambrian|Cambrian|||Of the Kangaroo Island Group.||||
17007|Smith Bay Shale|66761|5|Briefly described|p244, 246, 254|Cambrian|Cambrian|45 m identified in Investigator 1, where said to overlie Parara Limestone (contact may be faulted) and be overlain by White Point Conglomerate, but probably not at Emu Bay. Overlies the Stokes Bay Sandstone at Cape Cassini.||Of the Kangaroo Island Group.||||14-MAR-12
17007|Smith Bay Shale|67344|6|Mentioned|p260 Fig.1|Early Cambrian|Early Cambrian|Occurrence between Bald Rock and Hawk Nest is now regarded as a lithofacies within the lower White Point Conglomerate.||||||17-SEP-14
17007|Smith Bay Shale|69372|6|Mentioned|p27 fig. 5, p34 fig. 12|Cambrian|Cambrian|||Kangaroo Island Group|||Shale.|
17007|Smith Bay Shale|73107|5|Briefly described|Map legend.|Early Cambrian|Early Cambrian|Stansbury Basin. Fossils in the lower, shale facies include trilobite tracks and worm casts.|||||Lower shale facies: micaceous mudstone and siltstone; syneresis cracks, trough crossbeds and symmetrical ripples. Upper sandstone facies: massive and laminated cross-bedded sandstone; mud flakes; oolitic limestone towards the top.|
17007|Smith Bay Shale|73247|5|Briefly described|p204-207, p209-210|||Part of the western succession of the Kangaroo Island Group. Contains trilobites Redlichia takooensis and Balcoracania dailyi. This fossil evidence is used to correlate the unit with the Marsden Sandstone (including Rouge Mudstone Member) and Emu Bay Shale from the eastern succession.||Kangaroo Island Group||Underlain by Stokes Bay Sandstone. Correlates to Marsden Sandstone and Emu Bay Shale. Equivalent to Boxing Bay Formation and Minlaton Formation.||
17007|Smith Bay Shale|75071|6|Mentioned|p213|Early Cambrian|Early Cambrian|Kangaroo Island.||||||
17047|Snowtown Sands|29395|2|Defined|p3|Miocene|Miocene|||||||
17047|Snowtown Sands|29396|6|Mentioned|p110|||||||||
17047|Snowtown Sands|29397|6|Mentioned|p423|||||||||
17047|Snowtown Sands|35689|6|Mentioned|Fig.33|||Stratigraphic correlation, St.Vincent Basin.||||||
17047|Snowtown Sands|41513|6|Mentioned|Fig.4|||||||||
17047|Snowtown Sands|61155|5|Briefly described|p4, p17|Middle Miocene|Early Miocene|Interbedded fluvio-lacustrine clastics. Age:~21-~12.5Ma. Thickness: 20m. Geological Province: St Vincent Basin.||||||
17118|South Maslin Sand|22525|5|Briefly described|p35,37||Eocene|||||||
17118|South Maslin Sand|22528|4|Described|p42-44 Figs 2-6||Middle Eocene|||||||
17118|South Maslin Sand|22541|4|Described|p 19, 21, Fig1|||||||||
17118|South Maslin Sand|22587|6|Mentioned|p79 Fig.7|Late Eocene|Middle Eocene|||||||
17118|South Maslin Sand|22822|6|Mentioned|p11|||||||||14-FEB-23
17118|South Maslin Sand|23331|5|Briefly described|1089 Fig.2|Eocene|Eocene|||||||
17118|South Maslin Sand|23489|4|Described|p43|Oligocene|Eocene|||||||
17118|South Maslin Sand|23802|5|Briefly described|p21 Fig. 2|||Carbonaceous, pyritic, and glauconitic sand with goethitic pellets.||||||18-DEC-06
17118|South Maslin Sand|29697|6|Mentioned|Table 7|||||||||
17118|South Maslin Sand|31655|6|Mentioned|Table 1|||Geology & hydrology||||||
17118|South Maslin Sand|32117|6|Mentioned|Fig.2|||||||||
17118|South Maslin Sand|32509|5|Briefly described|p9|||From drillhole||||||
17118|South Maslin Sand|34536|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
17118|South Maslin Sand|34898|6|Mentioned|Table 1|||||||||
17118|South Maslin Sand|37324|6|Mentioned|p11|||||||||
17118|South Maslin Sand|38107|4|Described|p25|||||||||
17118|South Maslin Sand|38662|6|Mentioned|p2|||||||||
17118|South Maslin Sand|39351|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
17118|South Maslin Sand|40238|6|Mentioned|p324|||||||||
17118|South Maslin Sand|40877|5|Briefly described|Fig.2|||||||||
17118|South Maslin Sand|41025|6|Mentioned|Fig.2|||||||||
17118|South Maslin Sand|41513|6|Mentioned|p43|||See also P46||||||
17118|South Maslin Sand|41515|6|Mentioned|p107|||||||||
17118|South Maslin Sand|41520|5|Briefly described|Fig.5|||||||||
17118|South Maslin Sand|42498|5|Briefly described|Map Legend|Eocene|Eocene|||||||
17118|South Maslin Sand|42506|5|Briefly described|Map legend|Eocene||Age Tertiary||||||
17118|South Maslin Sand|43053|5|Briefly described|Map Legend|Eocene|Paleocene|Fluvial to marginal marine siliceous sand. Geological Province: St Vincent Basin.||||||25-MAY-05
17118|South Maslin Sand|43258|5|Briefly described|Map Legend|Eocene|Paleocene|||||||
17118|South Maslin Sand|43298|5|Briefly described|Map Legend|Eocene|Paleocene|||||||
17118|South Maslin Sand|44133|4|Described|p167, 165 Fig. 10.11|Late Eocene|Middle Eocene|Geological Province: Saint Vincent Basin. Formerly South Maslin Sands. Thickness: 41m+. Overlies North Maslin Sand.  Interfingers with Clinton Formation.||||||02-APR-13
17118|South Maslin Sand|60538|5|Briefly described|p479 Fig. 18|Oligocene|Eocene|Geological Province: Saint Vincent Basin.||||||
17118|South Maslin Sand|60953|5|Briefly described|Map Legend|Eocene|Paleocene|Fluvial to marginal marine siliceous sand. Geological Province: Saint Vincent Basin.||||||
17118|South Maslin Sand|61108|5|Briefly described|map legend|Eocene|Paleocene|Fluvial to marginal marine siliceous sand. Geological Province: St Vincent Basin.||||||
17118|South Maslin Sand|64397|5|Briefly described|p233 Fig. 2|Middle Miocene|Middle Miocene|Ferruginous quartz sand, cross-bedded, glauconitic. Geological province: St Vincent Basin. Grouped together with North Maslin Sand as the informal Maslin Sands in Fig. 1, p232.||||||
17118|South Maslin Sand|65375|6|Mentioned|p34 Fig.7.|Eocene|Eocene|Shown on Fig. 7 as Upper Eocene.||||||
17118|South Maslin Sand|65891|6|Mentioned|p221 Fig.5, p222 Fig.7, p228 Fig.11.|Paleogene|Paleogene|Eastern St Vincent Basin. Bartonian age.||||||
17118|South Maslin Sand|66131|6|Mentioned|p242 Fig.2|Eocene|Eocene|Middle to Late Eocene in age (from p.242 Fig.2 - stratigraphic correlation chart).||||||
17118|South Maslin Sand|66194|5|Briefly described|P584|Late Eocene|Late Eocene|St Vincent Basin. Marginal marine.||||||09-MAR-12
17118|South Maslin Sand|67462|5|Briefly described|Map legend.|Eocene|Eocene|Eastern Saint Vincent Basin.||||||
17118|South Maslin Sand|68715|6|Mentioned|p31 Fig.5|Lutetian|Ypresian|St Vincent Basin.||||||
17118|South Maslin Sand|70660|4|Described|p3, p9-p13, p15, p19, p25-p26, p33, p46|Late Bartonian|Late Bartonian|See also the Maslin Sand. Deposited in a marginal marine environment. Sparse marine body fossils are present throughout. A type section and the fossil assemblage is briefly described. This unit exceeds 40m in thickness in the Adelaide Sub-basin and Willunga Embayment.||||Overlies the North Maslin Sand. Overlain by the Tortachilla Limestone.|Cross-bedded and clay draped glauconitic sands that are rich in goethite pellets.|
17118|South Maslin Sand|70722|5|Briefly described|p218|Middle Eocene|Middle Eocene|Of St. Vincent Basin.||||Overlain by Tortachilla Limestone. Underlain by North Maslin Sand.||
17118|South Maslin Sand|72450|5|Briefly described|Brochure, Brochure map|Eocene|Eocene|Deposited in estuaries. 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.||||Overlies the North Maslin Sand.||
17118|South Maslin Sand|73188|5|Briefly described|[See comments]|Middle Eocene|Middle Eocene|St Vincent Basin. Ferruginised disconformity surface between this unit and the North Maslin Sand. Deposited in marginal marine and estuarine environments. p: 314, 319-320, 334-335, 345, 351, 355-356, 359.||||Disconformably underlain by North Maslin Sand. Overlain by Tortachilla Limestone.|Estuarine sand, fluvial sand, coal. Contains goethitic pebbles.|
17164|Spilsby Suite|22489|5|Briefly described|p12, p13|Calymmian|Calymmian|||||||
17164|Spilsby Suite|22494|5|Briefly described|p35|Calymmian|Calymmian|||||||
17164|Spilsby Suite|22629|5|Briefly described|p163, figs1,2|Calymmian|Calymmian|Age: 1510+/-12Ma||||||
17164|Spilsby Suite|23054|6|Mentioned|p10,32|||||||||
17164|Spilsby Suite|23481|5|Briefly described|p19 Fig 1|||Geological Province: Gawler Craton.||||||
17164|Spilsby Suite|23803|5|Briefly described|p29 Fig. 2|Paleoproterozoic|Paleoproterozoic|Age: ~`510Ma. Geological Province: Gawler Craton.||||||07-NOV-08
17164|Spilsby Suite|23805|5|Briefly described|p4 Fig. 1|Mesoproterozoic|Mesoproterozoic|Geological Province: Gawler Craton.||||||
17164|Spilsby Suite|24422|6|Mentioned|p84 Fig. 1|Mesoproterozoic|Mesoproterozoic|Geological Province: Gawler Craton.||||||
17164|Spilsby Suite|24505|5|Briefly described|p5 Fig. 1|||Geological Province: Gawler Craton.||||||
17164|Spilsby Suite|24508|5|Briefly described|p30|Mesoproterozoic|Mesoproterozoic|Age: ~1510Ma - youngest rocks in the Gawler Craton. Geological Province: Gawler Craton.||||||
17164|Spilsby Suite|24526|5|Briefly described|p97 Fig. 3, p100|Mesoproterozoic|Mesoproterozoic|Granitoid.  Age: 1510Ma.  Geological Province: Gawler Craton.||||||
17164|Spilsby Suite|24597|5|Briefly described|p526 Fig. 1|Mesoproterozoic|Mesoproterozoic|Geological Province: Gawler Craton.||||||
17164|Spilsby Suite|40448|5|Briefly described|p35 Table4|||Unnamed granites of this suite intrude Donington Granitoid Suite on Sir Joseph Banks Group islands.|1650+/-35Ma, 1576+/-199Ma|Of Lincoln Complex|Includes Middle Camp Granite|||12-AUG-10
17164|Spilsby Suite|41667|4|Described|p11|||||||||
17164|Spilsby Suite|43052|5|Briefly described|Table 5.6|||Shown on table of Hiltaba Suite granitoids, but see also p139.||||||
17164|Spilsby Suite|43053|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|||||||26-MAY-05
17164|Spilsby Suite|43258|5|Briefly described|Map Legend||Mesoproterozoic|||||||
17164|Spilsby Suite|43298|6|Mentioned|Map Legend||Mesoproterozoic|||||||
17164|Spilsby Suite|50605|5|Briefly described|p(iii), 11.2|Mesoproterozoic|Mesoproterozoic|Geological Province: Gawler Craton & Curnamona Province. Age: ~1530Ma.||||||
17164|Spilsby Suite|60515|6|Mentioned|p116 Fig.1 |||||||||
17164|Spilsby Suite|60657|5|Briefly described|p13 Fig. 2|Mesoproterozoic|Mesoproterozoic|Age: ~1500Ma. Geological Province: Gawler Craton.||||||10-MAY-05
17164|Spilsby Suite|60953|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Age: 1510Ma. Anorogenic granitoids.||||||
17164|Spilsby Suite|60958|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Granite. Age: ~1510 +/- 12Ma. Geological Province: Gawler Craton.||||||
17164|Spilsby Suite|61070|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Undifferentiated granites. Intrudes Donington Suite. Massive to moderately foliated, locally folded. One age of 1510 +/- 12Ma (U-Pb Zircon) given. Geological Province: Gawler Craton.||||||12-JAN-10
17164|Spilsby Suite|61108|5|Briefly described|map legend|Mesoproterozoic|Mesoproterozoic|Anorogenic adamellite to granodiorite.||||||
17164|Spilsby Suite|61121|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Granite.  Interpreted to intrude the Donington Suite in Spencer Gulf. Age: ~1520+/-12Ma. Geological Province: Gawler Craton. On LINCOLN sheet.||||||
17164|Spilsby Suite|61307|5|Briefly described|p36 Fig. 17|Mesoproterozoic|Mesoproterozoic|Geological Province: Gawler Craton. See also p39 Fig. 19.||||||
17164|Spilsby Suite|61522|5|Briefly described|p5 Fig.1|||Geological Province: Gawler Craton.||||||
17164|Spilsby Suite|63020|5|Briefly described|p971|Mesoproterozoic|Mesoproterozoic|Age: 1.51Ga. Geological province: Gawler Craton.||||||
17164|Spilsby Suite|63398|5|Briefly described|p663 Fig. 2|Mesoproterozoic|Mesoproterozoic|Age: >1510Ma. Geological Province: Gawler Craton.||||||10-DEC-07
17164|Spilsby Suite|63866|5|Briefly described|p7, p31|Calymmian|Calymmian|Gawler Craton.|c. 1500 Ma (Fanning et al., 2007)|||||
17164|Spilsby Suite|64130|5|Briefly described|p1378 Fig.1, p1380 Fig.2, p1384  |Mesoproterozoic|Mesoproterozoic|SE Gawler Craton.|ca. 1510 Ma (Fanning et al., 2007).|||||
17164|Spilsby Suite|64313|5|Briefly described|p450|Mesoproterozoic|Mesoproterozoic|Granites were emplaced around 1500Ma. Geological province: Gawler Craton.||||||09-FEB-10
17164|Spilsby Suite|64576|6|Mentioned|p625 Fig. 2|Mesoproterozoic|Mesoproterozoic|Age: c. 1500Ma.||||||
17164|Spilsby Suite|64722|6|Mentioned|Fig. 2 p3-6, p14, 27|Calymmian|Calymmian|The youngest magmatic suite in the Gawler Province.|1500 Ma.|||||11-APR-12
17164|Spilsby Suite|64739|6|Mentioned|p264 Fig.1.|Mesoproterozoic|Mesoproterozoic|Gawler Craton.||||||
17164|Spilsby Suite|65375|5|Briefly described|p13, p23, p25, p49.|Mesoproterozoic|Mesoproterozoic||1510 +/- 12 Ma.||||Includes a pluton of porphyritic, medium-grained, equigranular adamellite with magmatic layering.|
17164|Spilsby Suite|65376|5|Briefly described|p8 Fig.1.1, p12, pp95-100. |Mesoproterozoic|Mesoproterozoic|Eastern Gawler Craton. Associated with minor molybdenite and scheelite mineralisation on Spilsby Island.|1497 +/- 13 Ma.|||Intrudes Donington Suite granitoids.|Tabular feldspar-bearing granite, fine-grained granite to aplite, granodiorite; magmatic layering common.|
17164|Spilsby Suite|65390|5|Briefly described|p23 Fig.3|Calymmian|Calymmian|Spencer Domain, Gawler Craton. Age of 1510 Ma given.||||||
17164|Spilsby Suite|65772|6|Mentioned|p229 Fig.2|Calymmian|Calymmian|~1500 Ma||||||
17164|Spilsby Suite|65922|6|Mentioned|p13 Fig. 4|||Gawler Craton.||||||
17164|Spilsby Suite|66302|6|Mentioned|p4 Fig.3, p43, p47||||~1490 Ma (Fanning et al, 2007)|||||
17164|Spilsby Suite|67058|6|Mentioned|p477 Fig. 1|Mesoproterozoic|Mesoproterozoic|||||||
17164|Spilsby Suite|67181|5|Briefly described|p616 Fig.1|Mesoproterozoic|Mesoproterozoic|Gawler Craton. References: Fairclough et al. 2003, Payne et al. 2003.|ca 1500 Ma|||||
17164|Spilsby Suite|67536|5|Briefly described|Map Legend|Calymmian|Calymmian|Gawler Craton.|ca. 1510 +/- 12 Ma||||Adamellite to granodiorite.|
17164|Spilsby Suite|67581|6|Mentioned|p44 Fig.8, p45||||1510 Ma; Fanning (1997).|||||
17164|Spilsby Suite|68131|5|Briefly described|p2 Fig.1, p40|Mesoproterozoic|Mesoproterozoic|Occurs on several small islands in Spencer Gulf; this is the first identification of the c.1500 Ma Suite on the mainland (Corny Point, Yorke Peninsula).|1509 +/- 9 Ma.|||Intrudes Donington Suite.|Coarse-grained porphyritic granites.|
17164|Spilsby Suite|69048|5|Briefly described|p2-3|Mesoproterozoic|Mesoproterozoic|Eastern Eyre Peninsula/Yorke Peninsula.|c.1500 Ma.|||||
17164|Spilsby Suite|69649|6|Mentioned|p6 Fig.4,, p41|||||||||
17164|Spilsby Suite|70025|6|Mentioned|p22|Mesoproterozoic|Mesoproterozoic|Geological province: Mawson Craton.||||||
17164|Spilsby Suite|70027|6|Mentioned|p56|Mesoproterozoic|Mesoproterozoic|Geological province: Gawler Craton.||||||
17164|Spilsby Suite|71129|6|Mentioned|p18|Calymmian|Calymmian|Geological Province: Spencer Domain, Gawler Craton.|1510 Ma|||||
17164|Spilsby Suite|71317|5|Briefly described|p16|Mesoproterozoic|Mesoproterozoic|Spencer Domain, Gawler Craton.|c. 1510 Ma|||||
17164|Spilsby Suite|71348|6|Mentioned|p201|Calymmian|Calymmian|Geological province: Gawler Craton.||||||
17164|Spilsby Suite|71534|6|Mentioned|p296|Calymmian|Calymmian|Geological province: Gawler Craton.||||||
17164|Spilsby Suite|71859|6|Mentioned|p4|||Spencer Domain.|c. 1510 Ma|||||
17164|Spilsby Suite|71862|5|Briefly described|p3, p5|||Southern Gawler Craton.|c. 1555-1530 Ma|||||
17164|Spilsby Suite|72090|6|Mentioned|p10|Calymmian|Calymmian|Spencer Domain, Gawler Craton.|c. 1510 Ma|||||
17164|Spilsby Suite|72459|5|Briefly described|p5, p8, p14|Mesoproterozoic|Mesoproterozoic|Gawler Craton. Limited to exposures on the few islands off the eastern coast of southern Eyre Peninsula. Associated with known mineralisation such as Cu-Au-U-REE and Pb-Zn mineralisation.|1510 +/- 12 Ma|||||
17164|Spilsby Suite|73026|5|Briefly described|p6, p9-10||||c. 1500 Ma||||Granite, grey, coarse-grained and porphyritic.|
17164|Spilsby Suite|73027|5|Briefly described|p6, p9-10|Mesoproterozoic|Mesoproterozoic|Southern Gawler Craton.|c. 1500 Ma||||Granite, grey, coarse-grained porphyritic.|
17164|Spilsby Suite|73092|6|Mentioned|p2-3, p44, p49|Calymmian|Calymmian|Gawler Craton, southern. Age is of magmatic crystallisation. Dated sample is fine grained granite from drillhole PBD28 (294-295.4 m); sample tentatively assigned to this unit based on similar ages.|1513 +/- 26 Ma||||May include pink, medium-grained granite.|
17164|Spilsby Suite|73122|5|Briefly described|p22, 42|Mesoproterozoic|Mesoproterozoic|Southern Eyre Peninsula and islands of the Spilsby Group. Associated with the Spilsby Event.|1500 Ma.||||Granites.|
17164|Spilsby Suite|73234|6|Mentioned|p19|Calymmian|Calymmian|Gawler Craton. Age from Fanning, Reid and Teale (2007).|c. 1500 Ma|||||
17164|Spilsby Suite|73493|5|Briefly described|p712, p716 Fig.3, p726 Fig.13, p727|Calymmian|Calymmian|Gawler Craton, southeast.|ca 1500 Ma, 1510 Ma||||Localised series of granitic plutons.|
17164|Spilsby Suite|73634|6|Mentioned|p2 Fig.1, p4|||Rankin et al. (2006). Spilsby Island, Eyre Peninsula.|1500 Ma.|||||
17164|Spilsby Suite|73644|5|Briefly described|p3|Mesoproterozoic|Mesoproterozoic|A-type granites. Intrudes as c. 1505 Ma post-deformational dykes on the southern Yorke Peninsula.|c. 1515 Ma|||Crosscuts Corny Point Paragneiss and Donington Suite||
17270|Stansbury Limestone|22643|5|Briefly described|fig3p187, fig6|Early Cambrian|Early Cambrian|||||||
17270|Stansbury Limestone|22766|5|Briefly described|Fig.2 p561|Early Cambrian|Early Cambrian|||||||
17270|Stansbury Limestone|23155|6|Mentioned|p9|||Equivalent to the Kalladeina Formation (eastern Warburton Basin).||||||
17270|Stansbury Limestone|23818|5|Briefly described|p87 Fig.33|Cambrian|Cambrian|||||||
17270|Stansbury Limestone|23981|5|Briefly described|p8-9 Fig. 4, p23, p33|Middle Cambrian|Middle Cambrian|Geological Province: Stansbury Basin (Yorke Peninsula). Presented only as Stansbury in Fig 4. Shallow sub-tidal deposits - dark grey pyritic ooid grainstone and flat to ripple-laminated lime mudstone. Max. thickness: 67.1m (Stansbury town).||||||
17270|Stansbury Limestone|24465|5|Briefly described|p345 Fig.2|Cambrian|Cambrian|Geological Province: Stansbury Basin.||||||19-JAN-05
17270|Stansbury Limestone|30374|6|Mentioned|Fig.3|||Middle Cambrian age. Correlation||||||
17270|Stansbury Limestone|30801|6|Mentioned|p5|||Table P5-6||||||
17270|Stansbury Limestone|33332|6|Mentioned|p11|||M.Camb.||||||
17270|Stansbury Limestone|33471|6|Mentioned|Fig.1|||||||||
17270|Stansbury Limestone|33972|6|Mentioned|p13|||||||||
17270|Stansbury Limestone|34612|6|Mentioned|Fig.33|||Correlation chart. Cambrian||||||
17270|Stansbury Limestone|35255|6|Mentioned|Fig.8|||||||||
17270|Stansbury Limestone|40856|6|Mentioned|Fig.23.6|||||||||
17270|Stansbury Limestone|42222|6|Mentioned|Table 1 P4|||||||||
17270|Stansbury Limestone|42225|4|Described|p225|||||||||
17270|Stansbury Limestone|42269|6|Mentioned|Fig.1 P335|||||||||
17270|Stansbury Limestone|44133|5|Briefly described|p4 Fig. 7.2, 17, 28|Early Cambrian|Early Cambrian|Geological Province: Stansbury Basin.||||||
17270|Stansbury Limestone|60958|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Medium-bedded nodular to flaggy silty limestone, ooid grainstone and thin siltstone interlayers. Basal wackestone with grit. Geological Province: Stansbury Basin.||||||14-APR-05
17270|Stansbury Limestone|61121|5|Briefly described|Map legend|Early Cambrian|Early Cambrian|Medium bedded nodular to flaggy silty limestone, ooid grainstone and thin siltstone interlayers; basal wackestone with grit.  Age is Toyonian. Geological Province: Stansbury Basin.||||||06-JUN-05
17270|Stansbury Limestone|62787|6|Mentioned|p82 Fig. 3|Cambrian|Early Cambrian|Geological Province: Stansbury Basin (SA).||||||07-FEB-11
17270|Stansbury Limestone|65375|4|Described|p27 Fig.5, p28 Fig.6, pp30-31. |Cambrian|Cambrian|No outcrops, but up to 67m thick in cores. Contains Redlichia and abundant small skeletal fossils of latest Toyonian age.||||Overlies Corrodgery Formation. At Port Julia, unconformably overlies Wallaroo Group. Is overlain by Moonan Formation.|Medium-bedded, nodular to flaggy silty limestone, ooid grainstone and thin siltstone interlayers.|
17270|Stansbury Limestone|71102|6|Mentioned|p254|||Of Stansbury Basin.||||||
17357|Stokes Bay Sandstone|7992|4|Described|166, 165, 167, 168|Early Cambrian|Early Cambrian|Of Point Marsden Group, beds. Overlies Adelaide System phyllites. Overlain by Emu Bay Shales. Thickness uncertain due to faulting may be  ~1000 feet. Massive medium-grained sandstone. Includes large slump structures||||||12-JAN-10
17357|Stokes Bay Sandstone|22581|4|Described|Fig.2,p37|||Of the Kangaroo Island Group. Thickness: 700 m. Overlies Mount McDonnell Formation. Overlain by Smith Bay Shale||||||02-JUL-08
17357|Stokes Bay Sandstone|22643|5|Briefly described|p191, fig3|Early Cambrian|Early Cambrian|||||||
17357|Stokes Bay Sandstone|22766|4|Described|Fig.2 p561, 563|Early Cambrian|Early Cambrian|||||||
17357|Stokes Bay Sandstone|22857|5|Briefly described|p88 Fig. 14.7A|Early Cambrian|Early Cambrian|Of the Kangaroo Island Group. Geological Province: Stansbury Basin.||||||
17357|Stokes Bay Sandstone|22858|6|Mentioned|Fig14.7ap88-9|Toyonian|Tommotian|||||||
17357|Stokes Bay Sandstone|23818|5|Briefly described|p104|||Underlying unit: Strangway Hill Formation. Max. thickness: 2000 ft.||||||18-APR-05
17357|Stokes Bay Sandstone|30377|6|Mentioned|p204|||||||||
17357|Stokes Bay Sandstone|30982|6|Mentioned|p435|||||||||
17357|Stokes Bay Sandstone|31314|6|Mentioned|p102|||Cambrian||||||
17357|Stokes Bay Sandstone|33332|6|Mentioned|p11|||L.Camb-See also Fig.4.||||||
17357|Stokes Bay Sandstone|33471|6|Mentioned|Fig.1|||||||||
17357|Stokes Bay Sandstone|34612|4|Described|p104|||||||||18-APR-12
17357|Stokes Bay Sandstone|35255|6|Mentioned|Fig.8|||||||||
17357|Stokes Bay Sandstone|36198|6|Mentioned|Fig.I.2|||||||||
17357|Stokes Bay Sandstone|38873|4|Described|Table 3|||See also Fig.8||||||
17357|Stokes Bay Sandstone|40856|6|Mentioned|Fig.23.6|||||||||
17357|Stokes Bay Sandstone|41947|6|Mentioned|Fig.2 P17|||||||||
17357|Stokes Bay Sandstone|42225|6|Mentioned|Fig.4 P224|||||||||
17357|Stokes Bay Sandstone|42242|6|Mentioned|p199|||||||||
17357|Stokes Bay Sandstone|42269|6|Mentioned|Fig.1 P335|||||||||
17357|Stokes Bay Sandstone|42270|6|Mentioned|p353|||||||||
17357|Stokes Bay Sandstone|44133|4|Described|p4 Fig. 7.2, 6, 9, 10|Early Cambrian|Early Cambrian|Geological Province: Stansbury Basin. Of the Kangaroo Island Group.  Transitionally overlies Mount McDonnell Formation; underlies Smith Bay Shale. Thickness: 700m.||||||02-JUL-08
17357|Stokes Bay Sandstone|62785|6|Mentioned|p44 Fig.1|Early Cambrian|Early Cambrian|North coast Kangaroo Island. Underlies Smith Bay Shale.||||||
17357|Stokes Bay Sandstone|64282|5|Briefly described|Map legend|Early Cambrian|Early Cambrian|Of Kangaroo Island Group. Geological Province: Stansbury Basin. Red-brown to orange arkose. Abundant trough cross-bedding, planar and slumped bedding. Thick beds with tabular foresets and convoluted bedding.||||||24-JUL-08
17357|Stokes Bay Sandstone|65375|5|Briefly described|p33.|Early Cambrian|Early Cambrian|||Unit in Kangaroo Island Group.||Overlies Mount McDonnell Formation. Is overlain by Smith Bay Shale.||
17357|Stokes Bay Sandstone|65624|5|Briefly described|map legend|Cambrian|Cambrian|Principally massive coarsely current and slump-bedded red and white sandstones and quartzites. Marbles and calcareous slates on Fleurieu Peninsula||||||12-JAN-10
17357|Stokes Bay Sandstone|65625|4|Described|p124, p103|Cambrian||Phyllites and quartzites. Thickness: ~1000 ft.||||Conformably overlies upper Proterozoic Adelaide System.|Red and white sandstones and quartzites. Slumping and cross-bedding characteristic. No fossils found.|18-FEB-11
17357|Stokes Bay Sandstone|65686|6|Mentioned|p411|Cambrian|Cambrian|Kangaroo Island||||||
17357|Stokes Bay Sandstone|65892|5|Briefly described|p9 Fig.4, p22 Fig.10. |Early Cambrian|Early Cambrian|North Coast of Kangaroo Island.||||Overlies Mount McDonnell Formation. Is overlain by Smith Bay Shale.||
17357|Stokes Bay Sandstone|65921|6|Mentioned|p1, p2 (map legend).|Cambrian|Cambrian|||Of the Kangaroo Island Group.||||
17357|Stokes Bay Sandstone|66761|5|Briefly described|p244, 246, 254|Cambrian|Cambrian|Of the Kangaroo Island Group at Cape Cassini.||||||
17357|Stokes Bay Sandstone|69372|5|Briefly described|p27 fig. 5, p34 fig. 12, p33, 37|Cambrian|Cambrian|Forms bedrock in some regions. Pebbles interpreted to be from this unit are found in Cape Jervis Formation.||Kangaroo Island Group||Underlies Cape Jervis Formation.|Metasandstone and sandstone. Shows glaciation striations and textures.|
17357|Stokes Bay Sandstone|73107|5|Briefly described|Map legend.|Early Cambrian|Early Cambrian|Stansbury Basin.|||||Red-brown to orange arkose; abundant trough cross-bedding, planar and slumped bedding. Thick beds with large tabular foresets and convoluted bedding.|
17357|Stokes Bay Sandstone|73247|5|Briefly described|p204-207, p209-210|||Part of the western succession of the Kangaroo Island Group.||Kangaroo Island Group||Underlain by Mount McDonnell Formation. Overlain by Smith Bay Shale. Equivalent to White Point Conglomerate and Minlaton Formation.||
17380|Stonyfell Quartzite|9124|5|Briefly described|Map Legend|Adelaidean|Adelaidean|In northern part of sheet. Dark pyritic shales, quartzitic and sandy at base.||||||
17380|Stonyfell Quartzite|22869|6|Mentioned|p42, Fig3||Neoproterozoic|||||||04-NOV-22
17380|Stonyfell Quartzite|22889|6|Mentioned|p35|Adelaidean|Adelaidean|Parent - Bungarider Subgroup.||||||
17380|Stonyfell Quartzite|23731|6|Mentioned|p28|||||||||
17380|Stonyfell Quartzite|23818|6|Mentioned|p60|||Equivalent to the Undalya Quartzite.||||||
17380|Stonyfell Quartzite|29697|6|Mentioned|p7|||||||||
17380|Stonyfell Quartzite|29776|6|Mentioned|p82|||||||||
17380|Stonyfell Quartzite|29835|6|Mentioned|p177|||||||||
17380|Stonyfell Quartzite|30782|6|Mentioned|Table 2|||Refers Adelaide 1M. Sheet (1951)||||||
17380|Stonyfell Quartzite|30801|6|Mentioned|p5|||Table P5-6||||||
17380|Stonyfell Quartzite|30807|6|Mentioned|p102|||Suggested map symbol||||||
17380|Stonyfell Quartzite|31923|6|Mentioned|p8|||||||||
17380|Stonyfell Quartzite|32031|6|Mentioned|p168|||Proterozoic. Fig. 1||||||
17380|Stonyfell Quartzite|32424|6|Mentioned|p16|||Former name of Undalya Qzt.||||||
17380|Stonyfell Quartzite|32724|6|Mentioned|Fig.1|||Torrensian. Correlation||||||
17380|Stonyfell Quartzite|33423|4|Described|p12|||See also P13.||||||
17380|Stonyfell Quartzite|33547|6|Mentioned|Fig.6|||||||||
17380|Stonyfell Quartzite|33577|6|Mentioned|p80|||Geol. map.||||||
17380|Stonyfell Quartzite|33659|5|Briefly described|p7|||Geology & hydrology.||||||
17380|Stonyfell Quartzite|33951|6|Mentioned|p5|||Now Undalya Qzt.||||||
17380|Stonyfell Quartzite|34308|6|Mentioned|p189|||||||||
17380|Stonyfell Quartzite|34320|6|Mentioned|Fig.|||Regional geology plan.||||||
17380|Stonyfell Quartzite|34535|6|Mentioned|Fig.19|||||||||
17380|Stonyfell Quartzite|34536|6|Mentioned|Map legend|Adelaidean|Adelaidean|Torrensian||||||
17380|Stonyfell Quartzite|34586|5|Briefly described|p28|||Torrensian||||||
17380|Stonyfell Quartzite|34958|6|Mentioned|p87|||||||||
17380|Stonyfell Quartzite|34980|6|Mentioned|p6|||||||||
17380|Stonyfell Quartzite|36835|4|Described|p31|||||||||
17380|Stonyfell Quartzite|37461|6|Mentioned|Table 5.I|||||||||
17380|Stonyfell Quartzite|38157|6|Mentioned|Table III|||||||||
17380|Stonyfell Quartzite|38926|6|Mentioned|p26|||||||||
17380|Stonyfell Quartzite|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Torrensian||||||
17380|Stonyfell Quartzite|39350|6|Mentioned|Map legend|Adelaidean|Adelaidean|Torrensian||||||
17380|Stonyfell Quartzite|39351|6|Mentioned|Map legend|Adelaidean|Adelaidean|Torrensian||||||
17380|Stonyfell Quartzite|40003|5|Briefly described|p57|||See also Table 16||||||
17380|Stonyfell Quartzite|40442|6|Mentioned|p8|||||||||
17380|Stonyfell Quartzite|40456|6|Mentioned|Fig.2|||||||||
17380|Stonyfell Quartzite|40500|6|Mentioned|p142|||||||||
17380|Stonyfell Quartzite|40852|6|Mentioned|Fig.3.2|||||||||
17380|Stonyfell Quartzite|41403|6|Mentioned|p72|||||||||
17380|Stonyfell Quartzite|41404|4|Described|p107|||||||||
17380|Stonyfell Quartzite|41494|6|Mentioned|p30|||||||||
17380|Stonyfell Quartzite|41526|6|Mentioned|p47|||||||||
17380|Stonyfell Quartzite|42093|5|Briefly described|p6|||See also Fig.2||||||
17380|Stonyfell Quartzite|42098|5|Briefly described|Table 2 P54|||||||||
17380|Stonyfell Quartzite|42222|6|Mentioned|p14|||||||||
17380|Stonyfell Quartzite|42243|5|Briefly described|p211|||||||||
17380|Stonyfell Quartzite|42505|5|Briefly described|Map legend|Adelaidean (Torrensian)|Adelaidean (Torrensian)|||||||
17380|Stonyfell Quartzite|42506|5|Briefly described|Map legend|Adelaidean (Torrensian)||||||||
17380|Stonyfell Quartzite|42733|6|Mentioned|map legend|Adelaidean||||||||
17380|Stonyfell Quartzite|43052|5|Briefly described|p181,Table 6.1|||||||||
17380|Stonyfell Quartzite|43190|5|Briefly described|p32,Fig.3 p30.|||See also misspelling. Stoneyfell Quartzite,Fig.2.||||||
17380|Stonyfell Quartzite|50615|5|Briefly described|p303 Fig. 2, p305|||Geological Province: Adelaide Fold Belt. See also p306 Fig. 4||||||19-AUG-04
17380|Stonyfell Quartzite|61307|5|Briefly described|p25 Fig. 14|Torrensian|Torrensian|Of the Burra Group. Geological Province: Adelaide Fold Belt.||||||
17380|Stonyfell Quartzite|64647|6|Mentioned|p40|||Feldspathic quartzite.||||||
17380|Stonyfell Quartzite|65379|5|Briefly described|p643, p644|Neoproterozoic|Neoproterozoic|Of Burra Group (Warrina Supergroup). Quartzite, feldspathic, with shale interbeds; silty sandstone in part schistose and calcareous. N.B.  Asbestos deposit host, contains Kenton Valley asbestos mine.||||||
17380|Stonyfell Quartzite|71240|14|Not recorded|p6, p9|||||||Correlated with Undalya Quartzite.||
17380|Stonyfell Quartzite|71529|14|Not recorded|p1, 3|||||||||
17380|Stonyfell Quartzite|72450|5|Briefly described|Brochure map|||||Burra Group|||Feldspathic quartzite, sandstone and siltstone.|
17380|Stonyfell Quartzite|73188|5|Briefly described|p308, p316, p323-328, p331, p338, p340|Neoproterozoic|Neoproterozoic|Mount Lofty Ranges. A comparatively more resistant rock type that composes Mount Lofty. [Misspelt as Stonyell Quartzite p339].||Bungarider Subgroup, Burra Group|Wattle Park Member, Slapes Gully Member, Greenhill Member|Underlain by Woolshed Flat Shale. Overlain by Saddleworth Formation. Equivalent to Undalya Quartzite.|Feldspathic and dirty sandstone.|
17451|Stuart Range Formation|13516|6|Mentioned|p147, fig 5|Early Permian|Early Permian|From Arkaringa Basin||||||
17451|Stuart Range Formation|22613|6|Mentioned|p18|||||||||
17451|Stuart Range Formation|22922|6|Mentioned|33 fig 2|||||||||
17451|Stuart Range Formation|23054|4|Described|p18-9|Sakmarian|Asselian|||||||
17451|Stuart Range Formation|23282|6|Mentioned|p84 Fig 6.2|||Equivalent or younger than Waitoona beds. of Arckaringa Basin.||||||
17451|Stuart Range Formation|23829|5|Briefly described|p371|Permian|Permian|Geological Province: Arckaringa Basin.||||||
17451|Stuart Range Formation|24112|5|Briefly described|p254 Fig.2|Early Permian|Early Permian|Geological Province: Arckaringa Basin||||||
17451|Stuart Range Formation|24396|6|Mentioned|p220 Fig.4|||||||||
17451|Stuart Range Formation|30544|6|Mentioned|p52|||||||||
17451|Stuart Range Formation|30924|6|Mentioned|Map legend|Sakmarian|Sakmarian|||||||
17451|Stuart Range Formation|32203|6|Mentioned|p8|||L.Perm.||||||
17451|Stuart Range Formation|32204|5|Briefly described|p5|||L.Perm. Refraction survey||||||
17451|Stuart Range Formation|33523|4|Described|p24|||||||||
17451|Stuart Range Formation|33525|2|Defined|p2|Early Permian|Early Permian|||||||
17451|Stuart Range Formation|33971|6|Mentioned|p35|||P36 refers Townsend & Ludbrook (1975)||||||
17451|Stuart Range Formation|33976|6|Mentioned|p9|||||||||
17451|Stuart Range Formation|35080|6|Mentioned|Fig.3|||||||||
17451|Stuart Range Formation|35149|5|Briefly described|Table 1|||||||||
17451|Stuart Range Formation|35315|6|Mentioned|p2|||Fossil assemblages||||||
17451|Stuart Range Formation|35845|6|Mentioned|Fig.25|||||||||
17451|Stuart Range Formation|36733|6|Mentioned|p14|||||||||
17451|Stuart Range Formation|37851|6|Mentioned|p12|||||||||
17451|Stuart Range Formation|37855|6|Mentioned|p4|||||||||
17451|Stuart Range Formation|37917|6|Mentioned|p469|||||||||
17451|Stuart Range Formation|38022|6|Mentioned|Fig.4|||||||||
17451|Stuart Range Formation|38604|6|Mentioned|Map legend|Permian|Carboniferous|Carboniferous - Permian||||||
17451|Stuart Range Formation|38605|4|Described|p19|||See also Table 3.||||||
17451|Stuart Range Formation|39265|6|Mentioned|Fig. 3|||||||||
17451|Stuart Range Formation|39352|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
17451|Stuart Range Formation|40637|6|Mentioned|Fig.2|||||||||
17451|Stuart Range Formation|40912|6|Mentioned|Map legend|Permian|Carboniferous|Carboniferous-Permian||||||
17451|Stuart Range Formation|41183|6|Mentioned|Fig.3 p308|||||||||
17451|Stuart Range Formation|41491|4|Described|p170|||||||||
17451|Stuart Range Formation|41689|6|Mentioned|Table 1|||||||||
17451|Stuart Range Formation|41950|6|Mentioned|Fig.3 P4|||||||||
17451|Stuart Range Formation|42102|6|Mentioned|p86|||||||||
17451|Stuart Range Formation|42465|5|Briefly described|Map Legend|||||||||
17451|Stuart Range Formation|42469|4|Described|p27|||||||||
17451|Stuart Range Formation|42491|6|Mentioned|p5|||Arckaringa Basin.||||||
17451|Stuart Range Formation|42546|5|Briefly described|Map legend|Permian|Carboniferous|||||||
17451|Stuart Range Formation|42547|6|Mentioned|p83|||||||||
17451|Stuart Range Formation|42578|6|Mentioned|Table 1 P124-125|||||||||
17451|Stuart Range Formation|42723|5|Briefly described|map legend|Permian||||||||
17451|Stuart Range Formation|42736|5|Briefly described|map legend|Permian|Carboniferous|||||||
17451|Stuart Range Formation|42816|4|Described|p17|||||||||
17451|Stuart Range Formation|43048|4|Described|Table 2.|||||||||
17451|Stuart Range Formation|43050|5|Briefly described|p6|||||||||
17451|Stuart Range Formation|43052|5|Briefly described|Table 2.1|||||||||
17451|Stuart Range Formation|43053|5|Briefly described|Map Legend|Permian|Carboniferous|Geological Province: Arckaringa Basin.||||||25-MAY-05
17451|Stuart Range Formation|43258|5|Briefly described|Map Legend|Permian|Carboniferous|||||||
17451|Stuart Range Formation|43298|6|Mentioned|Map Legend|Permian|Carboniferous|||||||
17451|Stuart Range Formation|43657|6|Mentioned|Fig.3,p4|Permian|Carboniferous|||||||
17451|Stuart Range Formation|43690|6|Mentioned|Fig.2,p157|||||||||
17451|Stuart Range Formation|43743|6|Mentioned|Fig.2,p33||Early Permian|||||||
17451|Stuart Range Formation|43840|5|Briefly described|Fig3 p12|Permian|Carboniferous|||||||12-JUL-16
17451|Stuart Range Formation|44109|5|Briefly described|p22 Fig. 28|||Geological Province: central Officer Basin.||||||
17451|Stuart Range Formation|44133|5|Briefly described|p65 Fig. 8.4, 73-74|Sakmarian|Asselian|Geological Province: Arckaringa Basin. Overlies Boorthanna Formation. Underlies: Mount Toondina Formation.||||||
17451|Stuart Range Formation|44289|5|Briefly described|Map Legend||Sakmarian|||||||
17451|Stuart Range Formation|44935|5|Briefly described|Map Legend|Permian|Carboniferous|Arckaringa Basin and Mulgathing Trough||||||
17451|Stuart Range Formation|60953|5|Briefly described|Map Legend|Permian|Carboniferous|Geological Province: Arcaringa Basin.||||||
17451|Stuart Range Formation|61108|5|Briefly described|map legend|Permian|Carboniferous|Glaciomarine, fluvioglacial and fluviolacustrine till, clay, silt, sand and gravel, indurated and coal-bearing in Ackaringa Basin. Geological Province: Arckaringa Basin.||||||
17451|Stuart Range Formation|62893|6|Mentioned|p18|||Arckaringa Basin.||||Equivalent to Coolardie Formation.||
17451|Stuart Range Formation|65194|5|Briefly described|p173 Fig.4.56|Permian|Permian|Basement to much of the Garford Palaeovalley, Gawler Craton.||||||
17451|Stuart Range Formation|65489|5|Briefly described|p137, p143, p151|Permian|Permian|Arckaringa Basin. 490m thick. Hydrocarbon source rock. Could provide an excellent seal.||||Overlies Boorthanna Formation. Is overlain by Mount Toondina Formation.||
17451|Stuart Range Formation|69004|6|Mentioned|p29|Permian|Permian|||||||
17451|Stuart Range Formation|69454|5|Briefly described|p38:4, 6|Sakmarian|Asselian|Arckaringa Basin.||||Lateral equivalent of Purni Formation.||12-JUL-16
17451|Stuart Range Formation|69673|6|Mentioned|p153 fig 125|||||||Overlain by Mount Toondina Formation, overlies Boorthana Formation||
17451|Stuart Range Formation|69946|3|Fully described|p2-3, p5-6, p36, p38, p44-45|Sakmarian|Asselian|Arckaringa Basin. Townsend and Ludbrook (1975); replaces the informal Stuart Range beds of Ludbrook (1967). Type section is the interval 516.6 - 777.2m in Cootanoorina 1, based on gamma ray and neutron log signatures of the mudrock. Thickness to 491m. Equivalent rocks, named 'Crown Point Formation Unit B' (New, 1988) occur above the Crown Point Formation in the Pedirka Basin. Early Permian marine sediments. Potential for oil shale.||||Overlies Boorthanna Formation conformably, and Crown Point Formation disconformably. Is overlain conformably by Mount Toondina Formation.|Grey to dark grey and sometimes brown, homogeneous mudstone; with minor white to grey, sub-rounded, fine- to medium-grained sandstone and mid to dark grey, thinly laminated, carbonaceous siltstone.|
17451|Stuart Range Formation|69948|6|Mentioned|Fig.4.18|||Pedirka Basin.||||Overlies Crown Point Formation. Is overlain by Mount Toondina Formation and (locally) Purni Formation.||
17451|Stuart Range Formation|70938|5|Briefly described|p807-808, p815|||Arckaringa Basin.|c.300 Ma.||||Fine to medium clastic detritus.|13-DEC-19
17451|Stuart Range Formation|71043|5|Briefly described|p106|||Gawler Craton.|||||Shale.|
17451|Stuart Range Formation|71342|3|Fully described|Ch4 p25, Ch5 p2-p6|Early Permian|Early Permian|Arckaringa Basin. Deposited in a quiet water, restricted marine environment on the basis of its uniform lithology and the presence of arenaceous foraminifera. Formalised by Townsend and Ludbrook (1975) to replace the informal Stuart Range beds proposed by Ludbrook (1967). A type section in drill core from Cootanoorina 1 is mentioned. Maximum thickness of 491m is recorded in the Lake Phillipson Bore. An equivalent unit in the Pedirka Basin is described in Ch5 p6. See also Ch5 p36, Ch5 p38, Ch5 p44-p45, Ch9 p18, Ch9 p21, Ch11 p6.||||Conformably overlies the Boorthanna Formation. Conformably overlain by the Mount Toondina Formation.|Homogenous mudstone with minor sandstone and siltstone. Sandstone is sub-rounded, fine to medium grained. Siltstone is micromicaceous, carbonaceous and thinly laminated.|
17451|Stuart Range Formation|72476|6|Mentioned|p36 Fig.9|||Arckaringa Basin. Time-temperature thermal history diagram.||||||
17451|Stuart Range Formation|72478|5|Briefly described|p8|Early Permian|Early Permian|Arckaringa Basin.  Marine transgressive unit.|c. 280-270 Ma|||Conformably overlies the Boorthanna Formation. Underlies the Mt Toondina Formation.|Generally homogeneous marine shale with minor siltstone and sandstone.|29-MAR-21
17451|Stuart Range Formation|73398|5|Briefly described|p4|||||||Overlies Boorthanna Formation. Is overlain by Mount Toondina Formation.|Arckaringa Basin. Shallow marine deposits.|
17466|Sturt Formation|30178|6|Mentioned|p20|||||||||
17466|Sturt Formation|37238|4|Described|p358|||Lithology||||||
17466|Sturt Formation|42272|6|Mentioned|p402|||||||||
17466|Sturt Formation|43190|5|Briefly described|Fig.3 p30.|||Late Proterozoic (Neoproterozoic)||||||
17466|Sturt Formation|68276|6|Mentioned|p68|Neoproterozoic|Neoproterozoic|"The ""Formation"" is omitted."||||||
17468|Sturt Tillite|9124|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Boulder Tillite. Quartzites and arkoses, locally pebbly with interbedded siltstones, locally calcareous.||||||
17468|Sturt Tillite|22510|5|Briefly described|table1, p38|||Mount Lofty Ranges .  Of the Yudnamutana Subgroup.||||||13-OCT-04
17468|Sturt Tillite|22581|6|Mentioned|p44||Neoproterozoic|||||||
17468|Sturt Tillite|23562|5|Briefly described|p295 Fig 2|Cryogenian|Cryogenian|||||||
17468|Sturt Tillite|23818|5|Briefly described|p61 Fig.20, p64 Fig.22|||Underlain by Belair Sub-Group. Of the Umberatana Group. Geological Province: Adelaide Geosyncline.||||||05-DEC-06
17468|Sturt Tillite|23913|5|Briefly described|p110 Fig. 2|Adelaidean|Adelaidean|Geological Province: Sturt Shelf.  Of the Umberatana Group. Overlain by Tapley Hill Formation.||||||05-DEC-06
17468|Sturt Tillite|24138|5|Briefly described|p10 Fig. 1.1|Precambrian|Precambrian|Geological Province: Adelaide Geosyncline.||||||05-DEC-06
17468|Sturt Tillite|24546|5|Briefly described|p2 - 3 Fig.2|Neoproterozoic|Neoproterozoic|Of Umberatana Group. Geological Province: Adelaide Fold Belt.||||||16-JAN-08
17468|Sturt Tillite|29697|6|Mentioned|p7|||||||||
17468|Sturt Tillite|29895|6|Mentioned|p473|||||||||
17468|Sturt Tillite|30178|6|Mentioned|p20|||||||||
17468|Sturt Tillite|30307|6|Mentioned|p213|||||||||
17468|Sturt Tillite|30378|6|Mentioned|p432|||||||||
17468|Sturt Tillite|30621|5|Briefly described|p501|||Thickness about 300m. near Adelaide.||||||05-DEC-06
17468|Sturt Tillite|30801|6|Mentioned|p5|||Sturtian. Table p5-6.||||||05-DEC-06
17468|Sturt Tillite|30807|6|Mentioned|p103|||Suggested map symbol||||||
17468|Sturt Tillite|31468|6|Mentioned|p13|||||||||
17468|Sturt Tillite|31923|6|Mentioned|p8|||||||||
17468|Sturt Tillite|31967|3|Fully described|p.4|||||||||
17468|Sturt Tillite|31970|6|Mentioned|p16|||||||||
17468|Sturt Tillite|32364|6|Mentioned|p18|||||||||
17468|Sturt Tillite|32510|6|Mentioned|Table 1|||||||||
17468|Sturt Tillite|32551|6|Mentioned|p101|||L.Sturtian. Lithology||||||
17468|Sturt Tillite|32724|6|Mentioned|Fig.1|||Sturtian. Correlation||||||
17468|Sturt Tillite|32778|4|Described|p93|||||||||
17468|Sturt Tillite|33026|6|Mentioned|p537|||||||||
17468|Sturt Tillite|33336|4|Described|p244|||||||||
17468|Sturt Tillite|33422|6|Mentioned|Map legend|Precambrian|Precambrian|||||||
17468|Sturt Tillite|33423|4|Described|p13|||Strat. p12.||||||05-DEC-06
17468|Sturt Tillite|33470|6|Mentioned|Table 1|||||||||
17468|Sturt Tillite|33474|6|Mentioned|Fig.2|||||||||
17468|Sturt Tillite|34535|6|Mentioned|p62|||Photograph. See p61.||||||05-DEC-06
17468|Sturt Tillite|34536|6|Mentioned|Map legend|Precambrian|Precambrian|Equiv.Sturtian||||||
17468|Sturt Tillite|34612|6|Mentioned|p118|||Precambrian||||||
17468|Sturt Tillite|34766|6|Mentioned|p58|||||||||
17468|Sturt Tillite|35255|6|Mentioned|p13|||||||||
17468|Sturt Tillite|35565|6|Mentioned|p15|||Geochemistry program.||||||05-DEC-06
17468|Sturt Tillite|35628|6|Mentioned|Table 2|||||||||
17468|Sturt Tillite|36253|6|Mentioned|Fig.3-2|||||||||
17468|Sturt Tillite|36731|6|Mentioned|p124|||||||||
17468|Sturt Tillite|37461|6|Mentioned|Table 5.I|||||||||
17468|Sturt Tillite|37932|3|Fully described|p541|||||||||
17468|Sturt Tillite|38157|6|Mentioned|Table IV|||||||||
17468|Sturt Tillite|38873|4|Described|Table 2|||||||||
17468|Sturt Tillite|39210|5|Briefly described|p49|||Age||||||
17468|Sturt Tillite|39344|6|Mentioned|Map legend|Precambrian|Precambrian|Sturtian||||||
17468|Sturt Tillite|39350|6|Mentioned|Map legend|Precambrian|Precambrian|Sturtian||||||
17468|Sturt Tillite|39351|6|Mentioned|Map legend|Precambrian|Precambrian|Sturtian||||||
17468|Sturt Tillite|39352|6|Mentioned|Map legend|Precambrian|Precambrian|Sturtian||||||
17468|Sturt Tillite|40003|6|Mentioned|Table 16|||||||||
17468|Sturt Tillite|40217|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
17468|Sturt Tillite|40228|5|Briefly described|Fig.1|||||||||
17468|Sturt Tillite|40442|6|Mentioned|p8|||||||||
17468|Sturt Tillite|40456|6|Mentioned|Fig.2|||||||||
17468|Sturt Tillite|40503|4|Described|p101|||||||||
17468|Sturt Tillite|40852|6|Mentioned|Fig.3.2|||||||||
17468|Sturt Tillite|40906|6|Mentioned|Fig.9|||||||||
17468|Sturt Tillite|41005|6|Mentioned|Fig.2|||||||||
17468|Sturt Tillite|41401|6|Mentioned|p32|||||||||
17468|Sturt Tillite|41404|6|Mentioned|p73|||||||||
17468|Sturt Tillite|41405|3|Fully described|p141|||||||||
17468|Sturt Tillite|41494|6|Mentioned|p34|||||||||
17468|Sturt Tillite|42222|6|Mentioned|p16|||||||||
17468|Sturt Tillite|42238|6|Mentioned|Table 1 P74|||||||||
17468|Sturt Tillite|42268|6|Mentioned|p331|||||||||
17468|Sturt Tillite|42505|5|Briefly described|Map legend|Adelaidean (Sturtian)|Adelaidean (Sturtian)|||||||
17468|Sturt Tillite|42731|6|Mentioned|map legend|Proterozoic||||||||
17468|Sturt Tillite|43052|5|Briefly described|Table 6.1|||||||||
17468|Sturt Tillite|44342|6|Mentioned|p.9|||SG/53-5.||||||
17468|Sturt Tillite|45155|6|Mentioned|p26|||||||||
17468|Sturt Tillite|46865|6|Mentioned|p44|||See also Table.2||||||
17468|Sturt Tillite|49027|6|Mentioned|p2|||||||||
17468|Sturt Tillite|60958|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Glacial diamictite of massive green-grey claystone with boulders or angular to rounded pebbles of metamorphic rocks, granite, quartzite and chert. Geological Province: Adelaide Geosyncline.||||||14-APR-05
17468|Sturt Tillite|61121|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Glacial diamictite of massive green-grey claystone with boulders or angular to rounded pebbles of metamorphic rocks, granite, quartzite and chert.  Geological Province: Adelaide Geosyncline.||||||
17468|Sturt Tillite|61732|5|Briefly described|p28 Fig. 13|Sturtian|Sturtian|Of the Yudnamutana Subgroup (Umberatana Group). Geological Province: Adelaide Rift Complex.||||||07-FEB-11
17468|Sturt Tillite|62903|6|Mentioned|p729, p730 Fig.1|Sturtian|Sturtian|Adelaide Rift Complex. Sturtian glaciation (Preiss et al. 1998) correlates with Areyonga Formation. Presented in text as Sturt-Appila-Pualco-Bolla Bollana-Merirjina Tillites. Presented in figure as Sturt/Applia.||Yudnamutana Subgroup||Sturtian glacial units overlain by Tapley Hill Formation||
17468|Sturt Tillite|64103|6|Mentioned|p397, p404|||Of Adelaide Rift Complex. May correlate with infomal units in the Vines Fm.||||||07-FEB-11
17468|Sturt Tillite|64282|5|Briefly described|Map legend|Neoproterozoic III|Neoproterozoic III|Geological Province: Adelaide Geosyncline. Glacial diamictite of massive, green-grey claystone with boulders or angular to rounded pebbles of metamorphic rocks, granite, quartzite and chert.||||||01-JUL-08
17468|Sturt Tillite|64796|6|Mentioned|p192|||||||||
17468|Sturt Tillite|64797|5|Briefly described|p153 Fig.2, p158, p164 Fig.11 |||See also p168 Tb.11, p169 Fig.12, p173. International correlations.||||||
17468|Sturt Tillite|65375|4|Described|p7, p25. |Neoproterozoic|Neoproterozoic|Sediments deposited along the Torrens Hinge Zone marginal to Adelaide Geosyncline. Siltstone contains poorly preserved leiosphaeroidal acritarchs. Deposition in glacio-lacustrine setting, possibly with minor marine influence.||||Locally, unconformably overlies Rhynie Sandstone or Wallaroo Group.|Diamictite consisting of massive grey-green siltstone to claystone with angular to rounded boulders or pebbles of metamorphic rocks, granite, quartzite and chert; cross-bedded sandstone and massive to bedded siltstone intercalations in diamictite.|
17468|Sturt Tillite|67030|6|Mentioned|p409 Fig. 2|Cryogenian|Cryogenian|||||Underlies the Tapley Hill Formation; equivalent to the Wilyerpa Formation.||26-APR-12
17468|Sturt Tillite|68244|6|Mentioned|p671|Cryogenian|Cryogenian|South Australia.||||||
17468|Sturt Tillite|68270|5|Briefly described|p677-681,683|Cryogenian|Cryogenian|Adelaide Rift Complex. Correlable to Pirrilyungka Formation, Chambers Bluff Tillite, Areyonga Formation, Naburula Formation, Mount Cornish Formation and Yardida Tillite.||Unit of Umberatana Group.||||
17468|Sturt Tillite|69439|6|Mentioned|p24:7|||Adelaide Fold Belt.||||Correlated with Naburula Formation (Ngalia Basin).||12-JUL-16
17468|Sturt Tillite|69873|6|Mentioned|p82|||Adelaide Rift Complex. Included in diagram showing Cryogenian-Ediacaran stratigraphy and correlations with Tasmanian succession.||||||
17468|Sturt Tillite|70082|6|Mentioned|p2|Cryogenian|Cryogenian|Stuart Shelf and Kulpara-Adelaide region.||||||
17468|Sturt Tillite|71080|6|Mentioned|p3|Cryogenian|Cryogenian|Adelaide Rift Complex. Part of Supersequence 2.||||||
17468|Sturt Tillite|71129|6|Mentioned|p15|Tonian|Tonian|Of Stuart Shelf. Deposited during Sturtian Glaciation.||||||
17468|Sturt Tillite|71237|14|Not recorded|p9|||||||||
17468|Sturt Tillite|71238|14|Not recorded|p2, 9|||||||||
17468|Sturt Tillite|71529|14|Not recorded|p1, 2, 3|||Refer to Howchin, 1920, Sprigg (1946).   ~1000 ft thick.||||||
17468|Sturt Tillite|72450|5|Briefly described|Brochure, Brochure map|||Seen primarily in the Sturt and Onkaparinga Gorges north of McLaren Vale. Deformed by the Delamerian Orogeny.|ca. 660 Ma|Umberatana Group|||Massive, cleaved, pebbly and boulder siltstone.|
17468|Sturt Tillite|73086|6|Mentioned|p62, p158|||Adelaide Rift Complex.||||Correlates to Areyonga Formation.||
17468|Sturt Tillite|73107|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Adelaide Geosyncline.|||||Glacial diamictite of massive green-grey claystone with boulders or angular to rounded pebbles of metamorphic rocks, granite, quartzite and chert. Subsurface only.|
17468|Sturt Tillite|73180|6|Mentioned|p47, 48|Neoproterozoic|Neoproterozoic|Adelaide Hills, Sturt Creek. Sturt glaciation.||||Correlated with the Areyonga Formation.|Glaciogenic sediments.|
17468|Sturt Tillite|73188|5|Briefly described|p316, p325-326, p330|Neoproterozoic|Neoproterozoic|Mount Lofty Ranges. Forms and excellent marker horizon in boreholes.||Yudnamutana Subgroup, Umberatana Group|||Diamictite, sandstone, siltstone.|
17468|Sturt Tillite|73236|4|Described|p34-39, p41, p47|Cryogenian|Cryogenian|Glaciomarine; deposited in a shelf setting. Records South Australia's oldest glaciations. Oldest rocks in Hallett Cove map area, occurring only as erratics in the Cape Jervis Formation.|c. 670-660 Ma|Yudnamutana Subgroup, Umberatana Group, Heysen Supergroup||Overlain by Tapley Hill Formation (Nepouie Subgroup).|Diamictite with grey silty-sandy matrix and a wide variety of pebbles, cobbles and boulders.|
17468|Sturt Tillite|74367|6|Mentioned|p20-22||||714+/-28 Ma MDA|||||
17528|Sunderland Formation|22510|5|Briefly described|table1p37,41|||Reinstated to original rank.  Now considered to be early Marinoan in age.  Formerly Sunderland Member of Tapely Hill Formation.  Now of the Upalinna Subgroup.||||||13-OCT-04
17528|Sunderland Formation|23250|5|Briefly described|p1124  Fig.2||Cryogenian|of Umberatana Group. Correlate of Aralka Formation, Ringwood Member, Brighton Limestone and Angepena Formation equivalent.||||||
17528|Sunderland Formation|41405|6|Mentioned|p167|||||||||
17528|Sunderland Formation|43845|5|Briefly described|Fig3 p43||Neoproterozoic|In Umberatana Group||||||12-JUL-16
17528|Sunderland Formation|60959|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Of the Upalinna Subgroup. Grey-green calcareous siltstone and fine to medium grained sandstone. Coarse grained to pebbly sandstone and conglomeratic limestone at base.||||||
17528|Sunderland Formation|61236|6|Mentioned|p24 Fig. 1|Adelaidean|Adelaidean|||||||
17528|Sunderland Formation|62085|6|Mentioned|p20 fig 5|Cryogenian|Cryogenian|||Umberatana Group||||
17528|Sunderland Formation|62592|5|Briefly described|p50 Table 5.1.|Marinoan|Marinoan|Adelaide Geosyncline.||Basal unit in Upalinna Subgroup.||Is overlain by Etina Formation.|Siltstone, sandstone.|
17528|Sunderland Formation|64797|6|Mentioned|p153 Fig.2, p164 Fig.11, p169 Fig.12|Ediacaran|Ediacaran|Adelaide Rift Complex. Lithology/rank not shown on diagram.||||||
17528|Sunderland Formation|64801|6|Mentioned|p110 Fig.2, p111-112|Neoproterozoic|Neoproterozoic|Adelaide Rift Complex.||Umberatana Group.||Unconformably overlies Tapley Hill Formation.||
17528|Sunderland Formation|65892|5|Briefly described|p33 Fig.18.|Cryogenian|Cryogenian|||Unit in Umberatana Group.||Overlies Tapley Hill Formation. Is overlain by Etina Formation.||
17528|Sunderland Formation|67979|4|Described|p538, p529-p531, p537 Fig.8, p542-545|Marinoan||In Central Flinders Ranges. Deep marine. Presented as Sun. Fm. in Fig.8. See also Figs. 1, 2.||Upalinna Subgroup|Wockerawirra Dolomite Member|Gradationally overlain by Etina Formation; the upper Yankaninna Formation is considered a time-equivalent succession.|thick succession of relatively featureless fine-grained and finely laminated calcareous shales|22-SEP-14
17528|Sunderland Formation|70082|6|Mentioned|p2|Cryogenian|Cryogenian|Flinders Ranges.||||||
17528|Sunderland Formation|71237|14|Not recorded|p10, 18|||||||||
17528|Sunderland Formation|72449|5|Briefly described|p1, p2 Map Legend|Neoproterozoic|Neoproterozoic|Central Flinders Ranges. Erosional base.||||Overlies Tapley Hill Formation and underlies Etina Formation.|Grey-green calcareous siltstone and fine to medium grained sandstone. Includes coarse to pebbly sandstone and/or oolitic limestone, often conglomeratic with large clasts of limestone and siltstone. Slumping of beds is common in upper part.|
17528|Sunderland Formation|72473|6|Mentioned|p4|||||||||
17531|Sundown Group|6823|5|Briefly described|p203, 205, 208, 211, 218-221, 223,|Palaeoproterozoic|Palaeoproterozoic|Metamorophic ages of 1593 +/- 10 Ma and 1636 +/- 10 Ma are provided, along with a crystallisation age of 1636+/-10 Ma. All ages reported herein are derived from this study. See also p227, 230, 232-236.  See also Sundown Schist p235.|1636 +/- 10 Ma (SHRIMP U-Pb zircon)|Willyama Supergroup||||26-MAR-22
17531|Sundown Group|22463|6|Mentioned|22 fig 27|Statherian|Statherian|Parent Willyama Supergroup Geol province Broken Hill - Olary Domain||||||
17531|Sundown Group|22500|4|Described|p3, 4, 13  Fig 5||Statherian|Age 1690Ma. Of the Willyama Supergroup.||||||29-MAY-07
17531|Sundown Group|22553|5|Briefly described|fig2p77,p83|||||||||
17531|Sundown Group|22575|6|Mentioned|p179 Fig.2|||||||||
17531|Sundown Group|22588|6|Mentioned|p85|||||||||
17531|Sundown Group|22631|6|Mentioned|table1, p173|Statherian|Statherian|||||||
17531|Sundown Group|22771|5|Briefly described|Table12.2p45,47-48|||||||||
17531|Sundown Group|22857|4|Described|p45 Tb. 12.2, p388 App1 Tb.A1.1|Paleoproterozoic|Paleoproterozoic|Of the Willyama Supergroup. Predominantly non-graphitic metasediment. Max. thickness: 1500m (1400 in type section). Geological Province: Willyama Fold Belt.||||||07-NOV-08
17531|Sundown Group|22884|6|Mentioned|p40 Fig. 1, p46|||Geological province: Broken Hill Domain; but also contains the only constituent/formation in the Olary Domain, namely, Mustering Paddock Formation.||||||11-JUN-14
17531|Sundown Group|22959|6|Mentioned|p95||Paleoproterozoic|||||||07-NOV-08
17531|Sundown Group|22962|6|Mentioned|p74||Statherian|||||||
17531|Sundown Group|22963|5|Briefly described|p69||Paleoproterozoic|Broad correlation with the Mt Isa Llewellyn Creek Formation and the Georgetown (Qld) Daniel Creek Formation.||||||07-NOV-08
17531|Sundown Group|22964|6|Mentioned|p55,56||Proterozoic|||||||
17531|Sundown Group|22965|6|Mentioned|Fig 1||Statherian|||||||
17531|Sundown Group|22966|5|Briefly described|p2,3,4||Proterozoic|||||||
17531|Sundown Group|22967|5|Briefly described|p25,6,30,Fig14||Statherian|||||||
17531|Sundown Group|23025|6|Mentioned|Fig1p75|||||||||
17531|Sundown Group|23039|6|Mentioned|p166||Statherian|||||||
17531|Sundown Group|23160|6|Mentioned|fig1|||||||||
17531|Sundown Group|23223|5|Briefly described|p43|||Of the informal Upper Willyama Supergroup. Curnamona Province.||||||16-JUN-09
17531|Sundown Group|23248|5|Briefly described|Fig2p169|||||||||
17531|Sundown Group|23346|6|Mentioned|48|||||||||
17531|Sundown Group|23347|6|Mentioned|p54|||Geological province: Broken Hill Domain. Equivalent to Olary Domain rocks of the Strathearn Group.||||||24-MAR-09
17531|Sundown Group|23390|6|Mentioned|p8|||||||||
17531|Sundown Group|23391|6|Mentioned|p6|||||||||
17531|Sundown Group|23461|5|Briefly described|p202|||||||||
17531|Sundown Group|23565|6|Mentioned|p195|||||||||
17531|Sundown Group|24197|5|Briefly described|p62|||Of the Willyama Supergroup. Shallow marine sediments. Geological province: Broken Hill Block.||||||07-FEB-11
17531|Sundown Group|24307|4|Described|p974|Proterozoic|Proterozoic|||||||
17531|Sundown Group|38969|4|Described|p209|||||||||
17531|Sundown Group|39662|2|Defined|p431|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
17531|Sundown Group|39826|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
17531|Sundown Group|39828|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
17531|Sundown Group|39849|6|Mentioned|p87|||||||||
17531|Sundown Group|39883|6|Mentioned|p380|||||||||
17531|Sundown Group|40290|6|Mentioned|Fig.2|||||||||
17531|Sundown Group|40595|6|Mentioned|p86|||||||||
17531|Sundown Group|40822|6|Mentioned|Fig.2|||||||||
17531|Sundown Group|41093|4|Described|p253|||||||||
17531|Sundown Group|41145|5|Briefly described|p827|||||||||
17531|Sundown Group|41402|6|Mentioned|p37|||||||||
17531|Sundown Group|41630|5|Briefly described|p3|||See also p27.||||||10-OCT-06
17531|Sundown Group|41633|6|Mentioned|Fig.2.2|||||||||
17531|Sundown Group|41651|6|Mentioned|p189|||||||||
17531|Sundown Group|42261|6|Mentioned|Fig 1 P530|||||||||
17531|Sundown Group|42528|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
17531|Sundown Group|42529|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
17531|Sundown Group|42531|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
17531|Sundown Group|42537|4|Described|p14|||||||||
17531|Sundown Group|42595|6|Mentioned|Fig. 2 P5|||||||||
17531|Sundown Group|42720|5|Briefly described|map legend|Paleoproterozoic||Same as Sundown Group, NSW.||||||07-NOV-08
17531|Sundown Group|42813|6|Mentioned|p9|||||||||
17531|Sundown Group|42897|5|Briefly described|Fig.3, P321|||||||||
17531|Sundown Group|42942|6|Mentioned|p17|||of Willyama Supergroup||||||
17531|Sundown Group|43052|6|Mentioned|p98|||||||||
17531|Sundown Group|43086|6|Mentioned|Fig.3|||||||||
17531|Sundown Group|43263|6|Mentioned|Map Legend||Paleoproterozoic|||||||07-NOV-08
17531|Sundown Group|43265|5|Briefly described|Map Legend||Paleoproterozoic|Of the Willyama Supergroup.||||||07-NOV-08
17531|Sundown Group|43266|5|Briefly described|Map Legend||Paleoproterozoic|Of the Willyama Supergroup.||||||07-NOV-08
17531|Sundown Group|43269|5|Briefly described|Map Legend||Paleoproterozoic|Of Willyama Supergroup.||||||07-NOV-08
17531|Sundown Group|43270|5|Briefly described|Map Legend||Paleoproterozoic|Of the Willyama Supergroup.||||||07-NOV-08
17531|Sundown Group|43271|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
17531|Sundown Group|43272|5|Briefly described|Map Legend||Paleoproterozoic|Of the Willyama Supergroup.||||||07-NOV-08
17531|Sundown Group|43274|5|Briefly described|Map Legend||Paleoproterozoic|Of the Willyama Supergroup.||||||07-NOV-08
17531|Sundown Group|43485|6|Mentioned|2||Proterozoic|of Willyama Complex||||||
17531|Sundown Group|43572|6|Mentioned|Fig.3.2 p6|||||||||
17531|Sundown Group|43583|5|Briefly described|Table 1, p2138|||||||||
17531|Sundown Group|46598|4|Described|p304|||See also p302.||||||18-JAN-07
17531|Sundown Group|50045|4|Described|p115 Fig. 2, p116 Fig. 3|Statherian|Statherian|Geological Province: Broken Hill Block. Of the Willyama Supergroup. Overlain by Paragon Group; underlain by Broken Hill Group. Age: 1640 Ma.||||||31-MAY-07
17531|Sundown Group|50606|5|Briefly described|p1.1|||Geological Province: Broken Hill Block. Of the Willyama Supergroup.||||||
17531|Sundown Group|50619|5|Briefly described|p174 Fig. 1|Paleoproterozoic|Paleoproterozoic|Of the Willyama Supergroup. Psammite and pelite deposits. Conformably overlies the Broken Hill Group; conformably overlain by the Paragon Group. Geological Province: Broken Hill Block.||||||15-MAY-13
17531|Sundown Group|60485|5|Briefly described|p28 Fig. 2|Statherian|Statherian|Age: <1672+/-7Ma. Equivalent to Saltbush Subgroup (Olary Domain). Geological Province: Broken Hill Domain.||||||15-MAY-13
17531|Sundown Group|61262|5|Briefly described|p455 Fig. 11|Paleoproterozoic|Paleoproterozoic|Age: <1700Ma. Geological Province: Broken Hill.||||||07-NOV-08
17531|Sundown Group|61606|5|Briefly described|p4 Fig. 2|Paleoproterozoic|Paleoproterozoic|Of the Willyama Supergroup.||||||07-NOV-08
17531|Sundown Group|61735|5|Briefly described|p649, p635 Fig. 1, p638, 639|Paleoproterozoic|Paleoproterozoic|Overlies Broken Hill Group. Age: 1680-1670Ma.  In the Euriowie Block. Includes psammites. See also p636 Fig. 2, p649-50.||||||04-JUN-15
17531|Sundown Group|61736|5|Briefly described|p666 Fig. 3|Paleoproterozoic|Paleoproterozoic|Ages for rocks within the group: </-1672+/-7Ma and </-1690Ma. Geological province: Broken Hill Domain.||||||
17531|Sundown Group|61908|5|Briefly described|p146|||Geological Province: Broken Hill Block.||||||
17531|Sundown Group|61936|6|Mentioned|p203|||Geological Province: Curnamona Province.||||||
17531|Sundown Group|62373|5|Briefly described|p503 Fig.2|Paleoproterozoic|Paleoproterozoic|Of the Willyama Supergroup. Geological Province: Curnamona Province/Olary Domain.||||||07-NOV-08
17531|Sundown Group|62473|5|Briefly described|p73-4|Paleoproterozoic|Paleoproterozoic|Max. age: 1670Ma. Geological province: Broken Hill Domain. Dominantly pelitic.||||||17-JUN-09
17531|Sundown Group|62535|5|Briefly described|p666 Fig.3, p671-674|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain.|<1672 +/- 7 Ma.|||Equivalent to the Saltbush Subgroup.|Mainly pelitic and psammopelitic schist with variable thin, planar psammite beds and occasional calc-silicate-rich ellipsoidal structures.|
17531|Sundown Group|62536|4|Described|p633, 635-636, 638-641, 649-650, 654|||See also p658-659. Broken Hill area. A variety of age determinations presented; depositional age remains uncertain. Metamorphosed c.1608-1598 Ma. Similar zircon provenance ages as Broken Hill Group and upper Paragon Group. Contains little stratiform mineralisation.|1788 +/- 8 Ma (MDA).||Cartwrights Creek Metasediments.|Overlies Broken Hill Group.|Layered, migmatised metasedimentary rocks.|
17531|Sundown Group|62592|5|Briefly described|p14, p15, p16 Fig.2.2.|||Broken Hill Domain, Curnamona Province. Equivalent to the Saltbush Group in the Olary Domain. Coeval with the northern Australian Pb-Zn basins; possibly prospective for Mount Isa and Century styles of mineralisation.|<1672 +/- 7 Ma.|Unit in Willyama Supergroup.||Overlies Broken Hill Group. Is overlain by Paragon Group.||
17531|Sundown Group|62728|5|Briefly described|p25 Fig. 2|||Geological Province: Curnamona Province.||||||07-FEB-11
17531|Sundown Group|62993|6|Mentioned|p35, p37|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain.||Willyama Supergroup||||19-DEC-21
17531|Sundown Group|63020|5|Briefly described|p987 Fig. 8|Paleoproterozoic|Paleoproterozoic|Geological Province: Curnamona Province (Broken Hill Domain).||||||07-NOV-08
17531|Sundown Group|63102|5|Briefly described|p9,13-14,32-34,39|Neoproterozoic|Neoproterozoic|Geological province: Broken Hill Domain, Curnamona Province.|<1672+\-7 Ma|||Equivalent to Walparuta Formation; Saltbush Subgroup.||
17531|Sundown Group|63110|6|Mentioned|p1129 Fig. 8|||Comprises pelitic to psammitic metasedimentary rocks.||||||11-JUN-08
17531|Sundown Group|63186|5|Briefly described|p66, p67,p70|Paleoproterozoic|Paleoproterozoic|Age: 1612+/-18 Ma and 1601+/-18 Ma (monzaite mean) and 1645 Ma. Geological Province: Broken Hill Domain, Curnamona Province.||||||07-NOV-08
17531|Sundown Group|63489|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Pelitic to psammitic metasediments. Geological Province: Broken Hill Domain; with unnamed equivalents in Olary Domain.||||||07-NOV-08
17531|Sundown Group|63519|5|Briefly described|p6 Fig. 2, p7|Paleoproterozoic|Paleoproterozoic|Overlain by Paragon Gp with sharp contact; overlies Broken Hill Gp. Age: <1690Ma. Metasediments, not strongly deformed and preserving sedimentary structures. Geol Prov: Broken Hill Block-Euriowie Block. See also p29 Fig. 11.||||||07-NOV-08
17531|Sundown Group|63866|4|Described|p36, p38, p40|||Broken Hill Domain, Curnamona Province. U-Pb zircon ages are derived from Page et al., 2005a and are interpreted as the maximum depositional ages for this group.|1688 +/- 6 Ma (U-Pb zircon) and 1672 +/- 7 Ma|Willyama Supergroup||Overlies the Hores Gneiss (Broken Hill Group). Equivalent to the Saltbush Group.|Thin-bedded, commonly graded pelite, psammopelite and psammite with calc-silicate nodules.|
17531|Sundown Group|64097|5|Briefly described|p302, p303|Paleoproterozoic|Paleoproterozoic|Of the Willyama Group. Underlies Paragon Group; overlies Broken Hill Group. Age: 1680-1670Ma. Mostly siliciclastic metasediments||||||07-FEB-11
17531|Sundown Group|64250|6|Mentioned|p25 fig 10|||Broken Hill Province.||Unit in Willyama Supergroup.||||
17531|Sundown Group|64316|5|Briefly described|p532, p533 Fig. 1|Paleoproterozoic|Paleoproterozoic|Of Willyama Supergroup. Overlain by Paragon Group. Lithology is progressively greater in pelitic-psammitic component upwards into this group.  Geological Province: Broken Hill Block||||||07-FEB-11
17531|Sundown Group|64722|5|Briefly described|Fig. 5 p.13|Statherian|Statherian|Broken Hill region, South Australian Craton.||Of Willyama Supergroup.||||11-APR-12
17531|Sundown Group|64725|6|Mentioned|p58 Fig.2. |||||||||
17531|Sundown Group|64741|5|Briefly described|p301 Fig. 4, p309, p310|Paleoproterozoic|Paleoproterozoic|Of Willyama Supergp.Overlies Broken Hill Gp. Age in upper levels:<1672+/-7Ma. Max.thickness: 1500m.Geol.prov: Broken Hill Domain. Comprises schistose interlayered psammopelite and pelite - more lith.detail (p309). Equiv.in Olary Domain is Walparuta Fm.||||||07-FEB-11
17531|Sundown Group|64742|5|Briefly described|p320, p323, pp327-328, p330. |||Broken Hill Domain. Major and trace element analyses, and Sm-Nd isotope data, are detailed.|<1672 Ma.|Unit in Willyama Supergroup.|||Psammites, calc-silicate rock.|
17531|Sundown Group|64743|5|Briefly described|pp339-340, pp342-344,  p346 Fig.7. |Paleoproterozoic|Paleoproterozoic|Broken Hill Block. Type section is c.1.35 km thick.|1690-1670 Ma.|Unit in Willyama Supergroup.||Overlies Broken Hill Group. Is overlain by Paragon Group.||
17531|Sundown Group|64744|5|Briefly described|p353 Fig.4, p356, p358. |Statherian|Statherian|Broken Hill Domain. Psammopelitic sediments.||Unit in Willyama Supergroup.||Overlies Broken Hill Group. Is overlain by Paragon Group.||
17531|Sundown Group|64944|5|Briefly described|p28 Fig. 1|Paleoproterozoic|Paleoproterozoic|Of Willyama Supergroup. Age at upper levels: <1672+/-7Ma. Geological province: Broken Hill Domain.||||||07-FEB-11
17531|Sundown Group|65681|6|Mentioned|p734 Fig.1.|||Broken Hill Block.||||||
17531|Sundown Group|65887|5|Briefly described|p51|||Primarily pelitic and psammo-pelitic metasediments. Thought to be deposited in a continental slope to deep water environment.||||||
17531|Sundown Group|66302|4|Described|p35, p36 Fig.9, p37, p39, p40, p73|Statherian|Statherian|Olary Domain, Curnamona Province. Ages are derived from Page et al. (2005).|1688 +/- 6 Ma to 1672 +/- 7 Ma|Willyama Supergroup||Equivalent to the Saltbush Group.|Thin-bedded, commonly graded mudstone, siltstone and sandstone with calcsilicate nodules.|
17531|Sundown Group|66857|6|Mentioned|p972 Fig.2.|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain.||Unit in Willyama Supergroup.||Overlies Broken Hill Group. Is overlain by Paragon Group.||
17531|Sundown Group|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Broken Hill Domain.|1672 +/- 7 Ma (maximum depositional age).|||Overlies Broken Hill Group.||
17531|Sundown Group|68067|6|Mentioned|Map legend.|||||||||27-AUG-13
17531|Sundown Group|68126|5|Briefly described|p6, p26, p29-30|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain, Curnamona Province.|~1685-1670 Ma (Page et al. in prep).|Willyama Supergroup.||Overlies Broken Hill Group. Is overlain by Paragon Group. Equivalent to Saltbush Group.||
17531|Sundown Group|68315|6|Mentioned|p766|||Broken Hill district, Curnamona Province. Cut by the Stephens Creek Shear Zone.|||||Upper amphibolite-facies metapelites and felsic gneisses.|
17531|Sundown Group|69999|5|Briefly described|p3,p7 Photo 4,p9 Photo 9,p12-15,p18,p20|Paleoproterozoic|Paleoproterozoic|Curnamona Province. Middle, rift-deepening, marine transgressive sedimentation with increased magmatic input. Represents much of the amphibolite facies for the Olarian Orogeny.||||||
17531|Sundown Group|70000|5|Briefly described|p31, p33-34, p36|Statherian|Statherian|Lithologically identical to upper part of Broken Hill Group, but lacks any syn-depositional igneous units.||Unit in Willyama Supergroup.||Overlies Broken Hill Group. Is overlain conformably by Paragon Group.|Interbedded pelite, psammopelitic and psammitic metasedimentary rocks.|
17531|Sundown Group|70014|5|Briefly described|Map legend|||Bedding well-developed within the metasediments, generally planar and continuous to lenticular. Graded bedding, small-scale cross-bedding, flame structures, and symmetrical and asymmetrical (climbing) ripple marks also present. Intrusive concordant and discordant K-feldspar-rich leucocratic rocks and intermixed pegmatite in some areas. Vary rare basic gneiss and quartz-gahnite rocks near the base. Rare finely-bedded quartz-tourmaline rocks and tourmaline schists also occur near the base. Zoned calc-silicate nodules are widespread in the metasediments.||Unit in Willyama Supergroup.||Overlies Broken Hill Group. Is overlain by Paragon Group.|Predominantly non-graphitic metasediment. Pelite-psammopelite units most abundant and more common in the lower half; psammite-psammopelite units more common in the upper half. Minor metasedimentary composite gneiss.|
17531|Sundown Group|70015|5|Briefly described|Map legend|Statherian|Statherian|Mineral deposits (if any) are shown.||Unit in Willyama Supergroup.||Overlies Broken Hill Group. Is overlain by Paragon Group.|Metapelite-metapsammopelite (abundant at base), and metapsammite-metapsammopelite (abundant at top); common calc-silicate ellipsoids; small basic gneiss and quartz-gahnite bodies at base.|
17531|Sundown Group|70405|6|Mentioned|p15, p29, p43 Table 3|Mesoproterozoic|Paleoproterozoic||1665 Ma-1680 Ma|Wilyama Supergroup||Correlated with Walparuta Formation||
17531|Sundown Group|70657|4|Described|p5, p6 Fig.1, p10 Fig.4, p11 Fig.5|Statherian|Statherian|See also p13 Fig.6, p14-15, p17, p33, p40, p44. Curnamona Province; Broken Hill, Mulyungarie, Olary Domains. Age inferred from Fig.4, but p15 suggests a minimum age c.1670 Ma. Fig.6 seems to suggest it includes Raven Hill Subgroup. With Broken Hill Group, is stratigraphically equivalent to Saltbush Group.|~1685-1655 Ma|Upper Willyama Supergroup.||Overlies Broken Hill Group. Underlies Cartwrights Creek Metasediments (Paragon Group). Equivalent to Walparuta Formation.||
17531|Sundown Group|70658|5|Briefly described|p2, 7, 15-16|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain, Curnamona Province.|<1672 +/- 7 Ma.|Willyama Supergroup.||Equivalent to Walparuta Formation.||
17531|Sundown Group|70858|6|Mentioned|p33|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain, Curnamona Province. Regarded by the authors as a good candidate for 1.75 Ga and younger detrital zircons in the Wernecke Supersuite, Yukon.||Willyama Supergroup.||||
17531|Sundown Group|71799|5|Briefly described|p150 fig 2|Statherian|Statherian|Curnamona Province.|ca 1650 Ma|||Overlain by the Cartwrights Creek Formation|Sandstone and greywacke.|
17531|Sundown Group|71968|4|Described|p1-13,18,28,41,45,47-48|Paleoproterozoic|Paleoproterozoic|Geological province: Curnamona province. Widespread in the Broken Hill Block. Page et al. (2005) reported maximum depositional ages of 1688+\-6 Ma in the Euriowie Block and 1672+\-7 Ma in the Monuments area. Sample GA 2676607 (sillimanite-rich psammite) yielded weighted mean 207Pb/206Pb ages of 1790+\-6 Ma and 1556+\-33 Ma, interpreted to be maximum depositional age of the psammite and minimum age for metamorphic zircon growth respectively. Reflects the usual spectrum of clastic zircon ages of the Willyama Supergroup.  Change from sliciclastic-dominated Sundown Group to fine-grained carbonaeous Paragon Group reflect a significant decrease (starving) in siliciclastic sediment input to the Curnamona Rift Basin; also reflects a change from older detrital zircons (c. 1792 Ma) in Sundown Group to younger populations in Paragon Group (c. 1754 Ma), possibly indicating a change in sediment source and supply and possibly exposure of a new source region based on relative sea level change.||Unit of Willyama Supergroup.||Overlain conformably by Paragon Group.|Predominantly metasediments, dominantly pelitic to psammopelitic rock units, with scattered calcsilicate nodules.|
17531|Sundown Group|72435|6|Mentioned|p715|Statherian|Statherian|Upper boundary with Paragon Group is gradational in places.|Between 1685 Ma and 1670 Ma|||Overlain by Paragon Group.||
17531|Sundown 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||||
17531|Sundown Group|72461|5|Briefly described|p5-6, p13, p16, p19|||||Willyama Supergroup||Overlies the Broken Hill Group. Overlain Conformably by the Paragon Group.|Sedimentary rocks.|
17531|Sundown Group|73243|6|Mentioned|p52-53, p58-59, p61, p67, p78-79|Statherian|Statherian|Broken Hill block-Euriowie block. Shown on p52 Fig.1 and p53 Fig.2.|~1670-1680 Ma|Willyama Supergroup|||Metasediments.|
17531|Sundown Group|73308|4|Described|p605-607, 611-618, 620, 622-623|||Broken Hill Block. Hydrothermal plumes are proposed as the source of much of these magnetite deposits.|c.1680-1670 Ma.|Willyama Supergroup.||Overlies Hores Gneiss (Broken Hill Group).|Metasediments (pelitic to psammitic schists) containing small amounts of bedding-controlled magnetite. Granulite facies metamorphism.|
17531|Sundown Group|73429|5|Briefly described|p106 Fig.2, p107|Statherian|Statherian|Curnamona Province. Broken Hill Domain, Mulyungarie Domain.||Willyama Supergroup, upper||Overlies Broken Hill Group||
17531|Sundown Group|73482|5|Briefly described|p419, p422 Fig.3, p423, p425-427, p430|Statherian|Statherian|Areas of stratigraphy are parallel to the andalusite-sillimanite isograd, in other areas the isograd crosses stratigraphy. See also p424 Fig.4, p428 Fig.7, p429 Fig.8, p432-434.|1670-1680 Ma|Willyama Supergroup||Overlies Broken Hill Group, underlies Paragon Group|Metasediments. Andalusite and silimanite metamorphic grades, partially melted in parts.|
17531|Sundown Group|73512|5|Briefly described|p2-3|Statherian|Statherian|Curnamona Province, Broken Hill Block. Represents deeper-water basin fill.||Willyama Supergroup||Underlain by Broken Hill Group. Overlain by Paragon Group.||
17531|Sundown Group|73524|6|Mentioned|p2, p5 Fig.3|||Rift-phase metasediments.||lower Willyama Supergroup||||
17531|Sundown Group|73575|5|Briefly described|p828 Fig.2, p829 Fig.3, p835-836, p841|Statherian|Statherian||1670-1680 Ma|Willyama Supergroup||Overlies Broken Hill Group, Purnamoota Subgroup, Hores Gneiss, underlies Paragon group, Cartwrights Creek Metasediments||
17580|Sweet Nell Shale|30310|6|Mentioned|Fig.1|||||||||
17624|Table Hill Volcanics|22517|6|Mentioned|P295||Neoproterozoic III|||||||
17624|Table Hill Volcanics|22650|6|Mentioned|p 159|Early Cambrian|Early Cambrian|Province - Officer Basin.||||||
17624|Table Hill Volcanics|22707|4|Described|P14, Table1 P8||Early Cambrian|Supersedes Officer Volcanics, Age of unit is 575+/-40 Ma.||||||12-NOV-08
17624|Table Hill Volcanics|22716|5|Briefly described|table4, p239|Early Cambrian|Neoproterozoic III|||||||
17624|Table Hill Volcanics|22814|5|Briefly described|p245, fig3|Neoproterozoic|Neoproterozoic|||||||
17624|Table Hill Volcanics|22907|6|Mentioned|39|||||||||
17624|Table Hill Volcanics|23282|6|Mentioned|p79|||Interpreted as synonym of Kulyong Volcanics.||||||
17624|Table Hill Volcanics|23328|5|Briefly described|1029|||Ages: 484+/-4 Ma K-Ar, 575+/-40 Rb-Sr.||||||07-SEP-09
17624|Table Hill Volcanics|23557|5|Briefly described|p96 Fig.2|Ordovician|Ordovician|Geological Province: Officer Basin.||||||
17624|Table Hill Volcanics|23571|4|Described|p3, 7|Ordovician|Ordovician|Geological Province: Officer Basin. Age: 484 +/- 4Ma. Underlying Unit:  Wahlgu Formation (conformable).||||||
17624|Table Hill Volcanics|23760|5|Briefly described|p25|Early Ordovician|Early Ordovician|||||||
17624|Table Hill Volcanics|23858|5|Briefly described|p919|Cambrian|Cambrian|Geological Province: Officer Basin.||||||
17624|Table Hill Volcanics|23914|6|Mentioned|p158 Fig. 12|||||||||
17624|Table Hill Volcanics|24067|5|Briefly described|p250|Cambrian|Cambrian|Geological Province: Officer Basin.||||||
17624|Table Hill Volcanics|24161|4|Described|p7, p9 Tb.6, p21|Early Ordovician|Early Ordovician|Age: 484 +/- 4 Ma. Unconformably overlies the McFadden Formation equivalent. Geological Province: Gunbarrel Basin.||||||
17624|Table Hill Volcanics|24390|5|Briefly described|p11 Fig. 6|Ordovician|Ordovician|Geological Province: Gunbarrel Basin.||||||
17624|Table Hill Volcanics|24578|5|Briefly described|p792|Cambrian|Cambrian|Age: ~510 Ma.||||||
17624|Table Hill Volcanics|30218|6|Mentioned|p404|||Age discussed||||||
17624|Table Hill Volcanics|30386|6|Mentioned|p8|||||||||
17624|Table Hill Volcanics|30388|4|Described|Table 1|||Table 1 P16. Correlated with Kulyong Volcanics. Ordovician?age.||||||
17624|Table Hill Volcanics|30390|4|Described|p198|||See also P199||||||
17624|Table Hill Volcanics|30944|6|Mentioned|Map legend|Ordovician|Ordovician|Prob. Ordovician||||||
17624|Table Hill Volcanics|30947|6|Mentioned|Map legend|Ordovician|Ordovician|Prob. Ordovician||||||
17624|Table Hill Volcanics|31455|6|Mentioned|p12|||||||||
17624|Table Hill Volcanics|31456|4|Described|Table 1|||||||||
17624|Table Hill Volcanics|31457|4|Described|Table 2|||||||||
17624|Table Hill Volcanics|31459|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
17624|Table Hill Volcanics|31460|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
17624|Table Hill Volcanics|31632|4|Described|Table 2|||See also P10||||||
17624|Table Hill Volcanics|31634|4|Described|Table 1|||||||||
17624|Table Hill Volcanics|31635|4|Described|Table 2|||||||||
17624|Table Hill Volcanics|31636|5|Briefly described|p7|||See also Table 2||||||
17624|Table Hill Volcanics|31638|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
17624|Table Hill Volcanics|31639|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
17624|Table Hill Volcanics|31641|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
17624|Table Hill Volcanics|31642|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
17624|Table Hill Volcanics|31914|3|Fully described|p96|||Same as Kulyong V. & Officer V.?||||||
17624|Table Hill Volcanics|32648|6|Mentioned|p32|||Ord.||||||
17624|Table Hill Volcanics|33478|6|Mentioned|Table 1|||||||||
17624|Table Hill Volcanics|33590|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
17624|Table Hill Volcanics|33591|5|Briefly described|p8|||||||||
17624|Table Hill Volcanics|33592|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
17624|Table Hill Volcanics|33595|4|Described|Table 1|||||||||
17624|Table Hill Volcanics|33625|6|Mentioned|p185|||P197||||||
17624|Table Hill Volcanics|34417|4|Described|p97|||Petrography P99. See also P101||||||
17624|Table Hill Volcanics|35123|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
17624|Table Hill Volcanics|35308|6|Mentioned|Table 1|||||||||
17624|Table Hill Volcanics|36096|6|Mentioned|Fig.3|||||||||
17624|Table Hill Volcanics|36257|6|Mentioned|Table 2.1|||||||||
17624|Table Hill Volcanics|36701|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
17624|Table Hill Volcanics|36888|6|Mentioned|p216|||||||||
17624|Table Hill Volcanics|36889|6|Mentioned|p219|||||||||
17624|Table Hill Volcanics|36890|4|Described|p404|||||||||
17624|Table Hill Volcanics|38329|6|Mentioned|Fig.1|||||||||
17624|Table Hill Volcanics|38898|6|Mentioned|p84|||||||||
17624|Table Hill Volcanics|43442|6|Mentioned|p16,21||Cambrian|Previously in Officer Basin||||||
17624|Table Hill Volcanics|43560|6|Mentioned|fig.1,p227|||||||||
17624|Table Hill Volcanics|43561|6|Mentioned|p1443|||||||||
17624|Table Hill Volcanics|43756|6|Mentioned|p542|||Rb-Sr age: 563+/-40 Ma||||||
17624|Table Hill Volcanics|44111|6|Mentioned|p.58, Fig. 2|||in Officer Basin, presented at "Table Hill" only in Fig. 2.||||||
17624|Table Hill Volcanics|44133|4|Described|p39|Middle Cambrian||More than 100m thick. Geological Province: Officer Basin. Age: ~570Ma (poorly constrained, Compston, 1974; Jackson and van de Graaff, 1981).||||||
17624|Table Hill Volcanics|44354|5|Briefly described|Map Legend||Early Cambrian|||||||
17624|Table Hill Volcanics|45104|6|Mentioned|p25|||||||||
17624|Table Hill Volcanics|45149|2|Defined|p34|Neoproterozoic|Neoproterozoic|See also p3 and table 1.||||||22-FEB-17
17624|Table Hill Volcanics|46975|6|Mentioned|p85|||||||||
17624|Table Hill Volcanics|49792|5|Briefly described|Fig.5|||Age 575 +- 40 Ma||||||
17624|Table Hill Volcanics|50085|5|Briefly described|p11 Fig. 6|Ordovician|Ordovician|Age: ~500Ma.  Geological Province: Officer Basin.||||||
17624|Table Hill Volcanics|50205|5|Briefly described|p59 Fig.1,|Ordovician|Ordovician|Of Gunbarrel Basin.|490-480 Ma|||||
17624|Table Hill Volcanics|50327|6|Mentioned|p309|||Basaltic volcanics in the interior of the Australia cration.||||||07-FEB-11
17624|Table Hill Volcanics|50621|5|Briefly described|p167|||Geological Province: Officer Basin.||||||
17624|Table Hill Volcanics|61023|5|Briefly described|p15 Fig. 8|Early Ordovician|Early Ordovician|Geological Province: Gunbarrel Basin.||||||11-APR-08
17624|Table Hill Volcanics|61272|5|Briefly described|p120, p123|Ordovician|Ordovician|Age: 484 +/- 4 Ma (K-Ar). Unconformably overlies the ?McFadden Formation. Overlain by the Lennis and Wanna Formations. See also p123 Fig.4||||||
17624|Table Hill Volcanics|61716|6|Mentioned|p650|Cambrian|Cambrian|Age: 500+/-7Ma (K-Ar, Veevers 2000).||||||
17624|Table Hill Volcanics|61732|5|Briefly described|p4 Fig. 3, p84|Early Ordovician|Cambrian|Basalts. Unconformable on Wahlgu Formation.  Age: 484+/-4Ma (Stevens and Apak 1999). Max. thickness: >483m. Geological Province: eastern Officer Basin.|Age: 484+/-4Ma (Stevens and Apak 1999).|||||07-FEB-11
17624|Table Hill Volcanics|62234|5|Briefly described|p130|Early Ordovician|Late Cambrian|Minimum crystallisation age yielded by plagioclase from evolved dolerite (diabase) lithology: 500.1+/-7Ma (K-Ar). Samples from Nyaninya sill: thin sections found to contain rare zirconolite grains intergrown with matrix feldspar, quartz and chlorite.||||||05-FEB-07
17624|Table Hill Volcanics|62453|4|Described|p5 Fig. 3, 19, 22, 70|Late Cambrian|Middle Cambrian|Geological Province: Officer Basin. Underlies: Lennis Sandstone. Overlies: Lungkarta Formation.||||||
17624|Table Hill Volcanics|62557|5|Briefly described|p461,462,463|Late Cambrian|Middle Cambrian|K/Ar age 500+/-14 Ma (Veevers,2000). Composition likely to be affected by alteration.||||||14-SEP-09
17624|Table Hill Volcanics|62987|5|Briefly described|p30|Middle Cambrian|Middle Cambrian|Geological Province: Gunbarrel Basin.||||||25-NOV-13
17624|Table Hill Volcanics|63022|5|Briefly described|p1013|Silurian?|Middle Cambrian|Coeval with Antrim Plateau Volcanics. Age: 484+/-8Ma (age of alteration not crystallisation). Geological province: Officer Basin.|484+/-8Ma age of alteration, not crystallisation|||||24-NOV-09
17624|Table Hill Volcanics|64068|6|Mentioned|p81|Cambrian|Cambrian|Officer Basin.|500 +/- 7 Ma.|||||05-APR-12
17624|Table Hill Volcanics|64103|6|Mentioned|p398, p400 Fig. 3|Cambrian|Middle Cambrian|Geological Province: Gunbarrel Basin.||||||07-FEB-11
17624|Table Hill Volcanics|64325|5|Briefly described|p82 Fig. 2, p85, p86|Ordovician|Ordovician|Geological Province: Gunbarrel  Basin.||||||26-AUG-08
17624|Table Hill Volcanics|64580|4|Described|map legend||Middle Cambrian|Basalt (in part vesicular and/or amygdaloidal) in multiple flows; interbedded sandstone and siltstone.||||||09-DEC-08
17624|Table Hill Volcanics|64589|4|Described|dated_samples,chemistry files|Cambrian|Neoproterozoic|Basalt.  K-Ar on plagioclase, crystallization age 500.1+/-7.4 Ma. Same material dated by whole-rock and pyroxene Rb/Sr (Compston, 1974) 575+/-40 Ma. Outcrop Nyaninya Sill, Nano-SIMS on zirconolite, crystallization age 504+/-18 Ma. Geochemical analyses.||||||12-NOV-08
17624|Table Hill Volcanics|64772|5|Briefly described|p16|Cambrian|Cambrian|Geological province: Gunbarrel Basin. Significant and widespread magmatic event.||||||25-NOV-13
17624|Table Hill Volcanics|64793|6|Mentioned|p286 Fig.5|Paleozoic|Paleozoic|||||||
17624|Table Hill Volcanics|64970|5|Briefly described|p718, p719, p719 Fig. 2, p720|Ordovician|Cambrian|Underlain by McFadden Formation, angular unconformity. Geological Province: Officer Basin. Also on p721 Fig. 6, 7.||||||
17624|Table Hill Volcanics|65074|6|Mentioned|p358|||Officer Basin.||||Correlated with Antrim Plateau Volcanics.||
17624|Table Hill Volcanics|65102|4|Described|p366, Figure 4-41, p368-373, 370|Early Cambrian|Early Cambrian|Officer Basin. 30-164m. Correlated with Kulyong Volcanics in SA. Basalt flows separated by a thin sandstone unit; subaerial extrusion with intervals of fluvial clastics; unconformable on folded Proterozoic rocks; dated 575+/-40 Ma [Neoproterozoic]; type section east side of Table Hill, 26deg 28min S, 126deg 53min E.||||||
17624|Table Hill Volcanics|65106|5|Briefly described|p130-133|Early Ordovician|Late Cambrian|Samples from Nyaninya sill used in the NanoSIMS 50 ion microprobe. New dating from lead isotopes in zirconolite. The 506 Ma age agrees within error with the previous K-Ar age, demonstrating the capability of the instrument.|500.1 +/-7.4 Ma (K-Ar); 506 Ma.||||Late-stage evolved diorite (diabase).|
17624|Table Hill Volcanics|65313|5|Briefly described|p578|Early Ordovician|Early Ordovician|Dated 484 +/- 4 Ma (Stevens and Apak, 1999).||||Is overlain by Mount Chandler Sandstone.||26-MAR-12
17624|Table Hill Volcanics|65337|6|Mentioned|p95.|||Probably synonymous with Kulyong Volcanics. Possible correlative with Kalkarindji Volcanic Group.||||||
17624|Table Hill Volcanics|65363|6|Mentioned|p5 Fig.4, p7. |Early Ordovician|Cambrian|||||Overlies Lungkarta Formation.||
17624|Table Hill Volcanics|65365|5|Briefly described|p10 Fig. 4||Cambrian|Central Officer Basin||||||
17624|Table Hill Volcanics|65366|5|Briefly described|p23 Fig. 3||Cambrian|Central Officer Basin||||||
17624|Table Hill Volcanics|65410|5|Briefly described|p74.|||Equivalent to the northern Australian Antrim Plateau Volcanics. The age is a recalculation from Compston (1974) but is equivocal; the unit may be as young as Cambrian.|563 +/- 40 Ma.||||Flood basalts.|
17624|Table Hill Volcanics|65416|4|Described|p137, p138 Fig.3, p139 Fig.4, p144, p146|Late Cambrian|Middle Cambrian|Western Officer Basin, SW and NE margins. The basalt flows were previously named the Officer Volcanics in the WA section of the Basin. Part of Sequence Pz1. Eroded in Savory Sub-basin prior to deposition of Paterson Formation. Correlated with Kulyong Volcanics (SA) and Antrim Plateau Volcanics. Extends into SA and is mapped as Kulyong Volcanics near the state border; they constitute a single tholeiitic basalt suite.|575 +/- 40 Ma (Townson 1985).|||Unconformably overlies McFadden Formation and Wirrildar beds. Is overlain unconformably by Lennis Sandstone and Paterson Formation.|Porphyritic and amygdaloidal tholeiitic basalts; basal fluvial sandstones; a sandy, weathered interval between two distinct massive subaerial flows.|
17624|Table Hill Volcanics|65506|5|Briefly described|p986|||Occurs in sedimentary rocks overlying Bangemall Supergroup in the east. Basalt, dolerite. Correlated with ~500 Ma Kalkarindji LIP.||||||23-MAY-17
17624|Table Hill Volcanics|66521|4|Described|p20.|Late Cambrian|Middle Cambrian|Gunbarrel and Officer Basins. Use of this Western Australian name was widened to include the South Australian unit formerly known as Kulyong Formation, because outcrop is more extensive and the unit is thicker and better understood in Western Australia.|K-Ar age of 484 +/- 4 Ma reflects alteration.||||Basalt; sediments.|
17624|Table Hill Volcanics|67195|4|Described|p5, p9 fig5, p10, p19 tbl1, p40,44,45,47|Cambrian|Cambrian|Basal Gunbarrel Basin. Thermal conductivities of 1.57 W/mK and 2.25 W/mK for the basalt and dolerite respectively.  Basal unit of one well in this study. See also App 1, App 2.||||Unconformably overlain by Lennis Sandstone, Wanna Formation, unconformably overlies Lupton Formation, Steptoe Formation|Includes reddish grey basalt and dolerite.|
17624|Table Hill Volcanics|67200|6|Mentioned|app 2 p9, 10||||||||Basalt and dolerite.|
17624|Table Hill Volcanics|67352|6|Mentioned|p31|||Part of the Kalkarindji Continental Flood Basalt Province, covering a vast area of NT-QLD-WA with an average thickness of .5 km.||||||
17624|Table Hill Volcanics|67454|6|Mentioned|p564.|Early Paleozoic|Early Paleozoic|Occupies a higher stratigraphic level than Wahlgu Formation, in Empress 1A drillhole.||||||
17624|Table Hill Volcanics|68902|6|Mentioned|p20, p27|Early Cambrian|Early Cambrian|Base of Gunbarrel Basin. Fed by c.500 Ma dolerite intrusions along N-trending fractures in the Rudall Complex.||||||
17624|Table Hill Volcanics|69003|6|Mentioned|p60|Cambrian|Cambrian|Officer Basin.||||||
17624|Table Hill Volcanics|69029|6|Mentioned|p329|Ordovician|Ordovician|Of Officer Basin.||||Overlain unconformably by Lennis Sandstone. Underlain unconformably by Lupton Formation or McFadden Formation or Vines Formation.||
17624|Table Hill Volcanics|69091|5|Briefly described|p30 Fig.3.5, p35, p37, see comments|Late Cambrian|Late Cambrian|Officer Basin. Deformed by a salt diapir and creates distinct gravity peak at -79 mGal as it curves upwards towards surface, and broad gravity low also matches well with extent of this salt diapir at depth. Misspelled as Table Hills Volcanics on p45 and p182. See also p38 Fig.3.7, p41 Fig.3.8, p44-45, p81 Fig.4.17, p105-109, p115 Fig.5.14, p174 Fig.9.5, p176, p177 Fig.9.6, p181-182, p200 Fig.10.2.||||Overlain by Lennis Sandstone and Wanna Formation; overlies with angular unconformity Browne, Hussar and Kanpa Formations, or disconformably over Wahlgu and Lungkarta Formations.|Predominantly basalt flows.|
17624|Table Hill Volcanics|69153|6|Mentioned|500k_geologyp08_lut.csv||Middle Cambrian||||||Basalt (in part vesicular and/or amygdaloidal) in multiple flows; interbedded sandstone and siltstone|
17624|Table Hill Volcanics|69445|3|Fully described|p30:1, 5-7, 9, 16-17|Cambrian|Cambrian|Peers (1969). Officer Basin. Synonymous with Kulyong Volcanics. Up to 116m thick. Type section is the east side of Table Hill (26o28'S, 126o53'E) in TALBOT map area. Another age determination is of 500 +/- 14 Ma (K-Ar whole rock; reported in Veevers, 2000).|505 +/- 3 Ma (Ar40/Ar39: Evins et al., 2009).|Kalkarindji Suite.|Boondawari dolerite.|Overlies Trainor Hill Sandstone. Conformably overlies Wahlgu and Lungkarta Formations. Is overlain by Paterson, Lennis and Wanna Formations, Mount Chandler Sandstone.|Coeval basaltic and intrusive rocks.|12-JUL-16
17624|Table Hill Volcanics|70137|5|Briefly described|Map legend.|Cambrian|Cambrian|Officer Basin.|||||Basalt (in part vesicular and/or amygdaloidal) in multiple flows; minor interbedded sandstone and siltstone.|
17624|Table Hill Volcanics|70315|6|Mentioned|p23|||Considered part of the Kalkarindji province through geochemical, geochronological and stratigraphic correlation.||||||
17624|Table Hill Volcanics|70634|4|Described|100k_geologyp_lut,csv|Cambrian|Cambrian||508 Ma (Isotopic)||||Basalt (in part vesicular and/or amygdaloidal) in multiple flows; minor interbedded sandstone and siltstone|
17624|Table Hill Volcanics|70793|4|Described|GEOL_LUT_CSV files|Cambrian|Cambrian|Of Officer Basin (Phase 2). Of Kalkarindji Large Igneous Province. Events: Gondwana breakup-southern margin (100.5-93.9 Ma); Alice Springs Orogeny (450-295 Ma); Rodingan Movement (Alice Springs Orogeny phase 1) (450-420 Ma). See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop_lut.csv.|508+\-10 Ma; 505+\-3 Ma||||Basalt (in part vesicular and/or amygdaloidal) in multiple flows; minor interbedded sandstone and siltstone|
17624|Table Hill Volcanics|70802|4|Described|250k_pre_mesozoic_interpgeop_lut.csv|Cambrian|Cambrian|Of Officer Basin (Phase 2); Kalkarindji Large Igneous Province. Events: Gondwana breakup-southern margin (100.5-93.9 Ma); Alice Springs Orogeny (450-295 Ma); Rodingan Movement (Alice Springs Orogeny phase 1) (450-420 Ma).|508+\-10 Ma; 505+\-3 Ma||||Basalt (in part vesicular and/or amygdaloidal) in multiple flows; minor interbedded sandstone and siltstone|
17624|Table Hill Volcanics|70826|6|Mentioned|p7 tbl 3|Cambrian|Cambrian|Officer Basin.||||||
17624|Table Hill Volcanics|70839|6|Mentioned|p343|||Of East Officer Basin.||||Underlain by Trainor Hill Sandstone and Apamurra Formation.||
17624|Table Hill Volcanics|71146|5|Briefly described|p6, p9, p18, p21-p22|Cambrian|Cambrian|Officer Basin, Kalkarindji Large Igneous Province.|506 +/- 6 Ma|||Unconformably overlain by the Lennis Sandstone and Mount Chandler Sandstone. Overlies the Marla Group.|Volcanics.|
17624|Table Hill Volcanics|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||dolerite, andesite, basalt|
17624|Table Hill Volcanics|71268|4|Described|GEOL_LUT_CSV files|Cambrian|Cambrian|Of Officer Basin (Phase 2). Of Kalkarindji Large Igneous Province. Events: Gondwana breakup-southern margin (100.5-93.9 Ma); Alice Springs Orogeny (450-295 Ma); Rodingan Movement (Alice Springs Orogeny phase 1) (450-420 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.|508+\-10 Ma; 505+\-3 Ma||||Basalt in multiple flows; in part vesicular or amygdaloidal; minor interbedded sandstone and siltstone|
17624|Table Hill Volcanics|71800|6|Mentioned|p26 fig 3|Middle Cambrian|Early Cambrian|Officer Basin.||||||
17624|Table Hill Volcanics|72034|5|Briefly described|500k_interpgeop16_lut|Cambrian|Cambrian|Officer Basin (Phase 2).|508 +/-10 Ma max, 505+/-3 Ma min||||Basalt (in part vesicular and/or amygdaloidal) in multiple flows; minor interbedded sandstone and siltstone.|
17624|Table Hill Volcanics|73083|6|Mentioned|p3|Cambrian|Cambrian|[Superseded by or a constituent of the Kalkarindji Suite]. These rocks comprise one of a series of widely separated exposures of Cambrian basalt attributed to the Kalkarindji Continental Flood Basalt Province (Glass et al, 2013). Correlation was based on matching magnetic signatures.|||||Basalt.|
17694|Talisker Formation|22643|5|Briefly described|p186|Early Cambrian|Early Cambrian|||||||
17694|Talisker Formation|24465|4|Described|p353|Early Cambrian|Early Cambrian|Replaces Talisker Calc-siltstone. Overlies Backstairs Passage Formation, overlain by Tapanappa Formation. Of Kanmantoo Group. Dyson et al (1996) included unit in their Silverton Subgroup.||||||19-JAN-05
17694|Talisker Formation|35744|6|Mentioned|p3|||||||||
17694|Talisker Formation|40228|5|Briefly described|Fig.1|||||||||
17694|Talisker Formation|42271|6|Mentioned|Fig.5 P376|||||||||
17694|Talisker Formation|42788|5|Briefly described|Fig.14 P148|||of Kanmantoo Group||||||
17694|Talisker Formation|61046|5|Briefly described|p8 Fig. 2|Early Cambrian|Early Cambrian|Of Kanmantoo Group. Includes Nairne Pyrite Member and Cooalinga Member. Pyritic metasediments, schist, calcsilicate.||||||
17694|Talisker Formation|63848|6|Mentioned|p534 Fig.4.|||||Unit in Kanmantoo Group.|Includes Cooalinga Member.|||
17694|Talisker Formation|65664|5|Briefly described|p1096, p1100, p1101-6 Tabs.1-4, Fig.5|Early Cambrian|Early Cambrian|||Of Bollaparudda Subgroup.|Includes Cooalinga Member.|Unconformably overlies Backstairs Passage Formation. Overlain by Tapanappa Formation.||09-MAY-12
17694|Talisker Formation|65892|5|Briefly described|p9 Fig.4. |Middle Cambrian|Early Cambrian|Fleurieu Peninsula.||Unit in Kanmantoo Group.||Unconformably overlies Backstairs Passage Formation. Is overlain by Tapanappa Formation.||
17694|Talisker Formation|68735|6|Mentioned|p235 Fig.3|Early Cambrian|Early Cambrian|Fleurieu Peninsula.||Of the Kanmantoo Group.||||10-APR-17
17694|Talisker Formation|68993|6|Mentioned|p544 Fig.1|Early Cambrian|Early Cambrian|Fleurieu Peninsula.||Of the Kanmantoo Group.||||
17694|Talisker Formation|73188|6|Mentioned|p316|Early Cambrian|Early Cambrian|Mount Lofty Ranges.||Bollaparudda Subgroup, Kanmantoo Group|||Calc-siltstone, pyrite, basal sandstone, local conglomerate.|
17803|Tanunda Creek Gneiss|39880|6|Mentioned|p351|||||||||
17803|Tanunda Creek Gneiss|40501|6|Mentioned|p124|||||||||
17803|Tanunda Creek Gneiss|43190|6|Mentioned|Fig.1,p28.|||||||||
17803|Tanunda Creek Gneiss|44133|5|Briefly described|p56 Table 7.3|||Metamorphic and metasomatic alteration of Kanmantoo Group. May be S-Type.||||||
17803|Tanunda Creek Gneiss|61307|6|Mentioned|p12|||||||||
17803|Tanunda Creek Gneiss|68314|6|Mentioned|p755 Fig.6, p757|Early Cambrian|Early Cambrian|Delamerian Orogen. Age inferred from Fig.6.|513 +/- 5 Ma (Foden et al., 2004).|||||
17814|Tapley Hill Formation|9862|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Of the Umberatana Group. Dark laminated siltstones, coarse dolomitic sandstones, sandy dolomites and tillite.||||||
17814|Tapley Hill Formation|22510|5|Briefly described|p38,41,Table1p37|||Age: Sturtian. Rb-Sr whole rock age 750+/-63Ma, probably a maximum age.||||||
17814|Tapley Hill Formation|22581|6|Mentioned|p44||Neoproterozoic|||||||
17814|Tapley Hill Formation|22677|4|Described|p733, Fig.2 p735|Neoproterozoic|Neoproterozoic|Age of unit: 750+/-53 Ma.||||||20-FEB-07
17814|Tapley Hill Formation|22772|4|Described|p62,66,Table13.1|Neoproterozoic III|Neoproterozoic III|||||||
17814|Tapley Hill Formation|22829|6|Mentioned|P16|||||||||
17814|Tapley Hill Formation|22857|5|Briefly described|Tb. 13.1 (insert p70-71)|Sturtian|Sturtian|Of the Farina Subgroup (Umberatana Group). See also p62 and p66.||||||
17814|Tapley Hill Formation|22921|5|Briefly described|38|||||||||
17814|Tapley Hill Formation|22925|6|Mentioned|48|||Underlying unit Pandurra Formation||||||
17814|Tapley Hill Formation|22926|6|Mentioned|39 fig 2|Neoproterozoic|Neoproterozoic|Geol province Adelaide Geosyncline. Parent Umberatana Group||||||
17814|Tapley Hill Formation|23054|6|Mentioned|p14|||||||||
17814|Tapley Hill Formation|23211|6|Mentioned|p40|||||||||
17814|Tapley Hill Formation|23250|5|Briefly described|p1124  Fig.2||Cryogenian|Of Umberatana Group. In Central Flinders Ranges and Stuart Shelf. Correlate of Aralka Formation in central and Eastern Amadeus Basin.||||||07-DEC-06
17814|Tapley Hill Formation|23314|5|Briefly described|331 Fig.2|||||||||
17814|Tapley Hill Formation|23315|5|Briefly described|p346|Neoproterozoic|Neoproterozoic|Of the Middle Umberatana Group. Thick succession of thinly laminated and partly calcareous siltstone representing a major tramsgression after a period of glaciation.||||||07-FEB-07
17814|Tapley Hill Formation|23351|5|Briefly described|283|Neoproterozoic|Neoproterozoic|||||||
17814|Tapley Hill Formation|23394|5|Briefly described|Map legend|Proterozoic|Proterozoic|||||||
17814|Tapley Hill Formation|23411|6|Mentioned|Map Legend|||||||||
17814|Tapley Hill Formation|23445|5|Briefly described|p436 Fig.1|||||||||
17814|Tapley Hill Formation|23482|5|Briefly described|p9|Adelaidean|Adelaidean|||||||
17814|Tapley Hill Formation|23552|5|Briefly described|p89|||Dark bluish grey, slightly calcareous, laminated siltstone, host rock for Terowie Kimberlite field. Max. thickness: 1500 m.||||||
17814|Tapley Hill Formation|23562|5|Briefly described|p295 Fig 2|Cryogenian|Cryogenian|||||||
17814|Tapley Hill Formation|23719|4|Described|p26|Neoproterozoic|Adelaidean|See also page 25 table 7. Overlain by part of Farina Subgroup. Geological Province: Gawler Craton. Max. thickness: >300 m.||||||22-JUN-09
17814|Tapley Hill Formation|23731|5|Briefly described|p27, p28|Adelaidean|Adelaidean|||||||
17814|Tapley Hill Formation|23802|5|Briefly described|p21 Fig. 2|||Weathered basement -light grey-white kaolinitic clay with minor dark pyritic shale; fresh parts of formation - dark, laminated, pyritic silty shale.||||||
17814|Tapley Hill Formation|23806|5|Briefly described|p1122 Fig. 1|Neoproterozoic|Neoproterozoic|||||||
17814|Tapley Hill Formation|23818|4|Described|p64 Fig.22, p68|Neoproterozoic|Neoproterozoic|Of the Farina Sub-Group. Max. thickness: >10 000 ft (in some areas). Contains flat beds - limestone.||||||20-FEB-07
17814|Tapley Hill Formation|23913|4|Described|p108, p110 Fig. 2|Adelaidean|Adelaidean|Umberatana Group.  Age: 750 +/- 53 Ma (Rb-Sr).  Overlain by  "Yudnapinna Beds" and Etina Formation.  Underlain by  Sturt Tillite and Wilyerpa Formation.  Intruded by the Woocalla Dolomite Member.||||||07-DEC-06
17814|Tapley Hill Formation|24175|3|Fully described|p13|Neoproterozoic|Neoproterozoic|Of Farina Supbgroup (Umberatana Group).  Includes Tindelpina Shale Member as topmost layer.  Overlain by Brighton Limestone (in boreholes); unconformably underlain by Myrtle Springs Formation.Max. thickness: 800m.||||||14-DEC-06
17814|Tapley Hill Formation|24176|4|Described|p13, p25 Tb. 1|Adelaidean|Adelaidean|Of Farina Group.  Blue-grey shales, minor siltstones, conglomerates, blue-black pyritic shale.  Contains the Tindelpina Shale Member.  Intertongues with Balcanoona Formation.  Max. thickness: 1525m.  Geological Province: Mount Painter Province.||||||
17814|Tapley Hill Formation|24195|6|Mentioned|p48|||Geological Province: Adelaide Geosyncline||||||
17814|Tapley Hill Formation|24288|5|Briefly described|p33|Neoproterozoic|Neoproterozoic|Age: ~700Ma.||||||
17814|Tapley Hill Formation|24321|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Farina Subgroup.||||||07-DEC-06
17814|Tapley Hill Formation|24362|5|Briefly described|p42|Adelaidean|Adelaidean|||||||22-MAR-05
17814|Tapley Hill Formation|24364|6|Mentioned|p29 Fig.3|Neoproterozoic|Neoproterozoic|||||||
17814|Tapley Hill Formation|24476|4|Described|p547 Fig. 4|Adelaidean|Adelaidean|Overlies the Wilyerpa Formation and the Merinjina Tillite. Overlain by the Etina Formation and the "Yudnapinna Beds".  Geological Province: Adelaide fold belt and Stuart Shelf||||||07-DEC-06
17814|Tapley Hill Formation|24546|5|Briefly described|p2 - 3 Fig.2|Neoproterozoic|Neoproterozoic|Of Umberatana Group. Geological Province: Adelaide Fold Belt.||||||16-JAN-08
17814|Tapley Hill Formation|24584|5|Briefly described|p14 Fig. 2|Neoproterozoic|Neoproterozoic|Dolomitic siltstone.||||||
17814|Tapley Hill Formation|29656|4|Described|Fig.3|||||||||
17814|Tapley Hill Formation|29777|5|Briefly described|p88|||||||||
17814|Tapley Hill Formation|29778|6|Mentioned|p167|||||||||
17814|Tapley Hill Formation|29780|4|Described|p92|||||||||
17814|Tapley Hill Formation|29831|6|Mentioned|p175|||||||||
17814|Tapley Hill Formation|29837|4|Described|p61|||||||||
17814|Tapley Hill Formation|30052|6|Mentioned|Fig.5|||See also Fig.6. Proterozoic age.||||||
17814|Tapley Hill Formation|30053|6|Mentioned|p112|||Proterozoic age.||||||
17814|Tapley Hill Formation|30176|6|Mentioned|Map legend|Precambrian|Precambrian|Sturtian||||||
17814|Tapley Hill Formation|30177|4|Described|p76|||See also p77-79.||||||07-DEC-06
17814|Tapley Hill Formation|30178|6|Mentioned|p20|||||||||
17814|Tapley Hill Formation|30261|6|Mentioned|Table 1|||Sturtian - Marinoan age||||||
17814|Tapley Hill Formation|30376|6|Mentioned|p77|||||||||
17814|Tapley Hill Formation|30377|6|Mentioned|p201|||||||||
17814|Tapley Hill Formation|30378|6|Mentioned|p432|||||||||
17814|Tapley Hill Formation|30713|5|Briefly described|p106|||||||||
17814|Tapley Hill Formation|30799|6|Mentioned|p2|||Stratigraphy and terminology.||||||
17814|Tapley Hill Formation|30801|6|Mentioned|p5|||Table p5-6.||||||14-DEC-06
17814|Tapley Hill Formation|30802|5|Briefly described|Table 1|||Sturtian||||||
17814|Tapley Hill Formation|30807|6|Mentioned|p103|||Suggested map symbol||||||
17814|Tapley Hill Formation|31022|4|Described|Fig. 24|||||||||
17814|Tapley Hill Formation|31538|6|Mentioned|p172|||See also Fig. 1||||||
17814|Tapley Hill Formation|31541|6|Mentioned|p545|||||||||
17814|Tapley Hill Formation|31698|6|Mentioned|Map legend|Precambrian|Precambrian|Sturtian||||||
17814|Tapley Hill Formation|31923|6|Mentioned|p10|||||||||
17814|Tapley Hill Formation|32146|5|Briefly described|p366|||Refers metamorphism. Fig.3||||||
17814|Tapley Hill Formation|32364|6|Mentioned|p17|||||||||
17814|Tapley Hill Formation|32481|6|Mentioned|p8|||Stratigraphy described||||||
17814|Tapley Hill Formation|32506|6|Mentioned|p115|||||||||
17814|Tapley Hill Formation|32510|6|Mentioned|p104|||||||||
17814|Tapley Hill Formation|32547|6|Mentioned|Fig.2|||Sturtian||||||
17814|Tapley Hill Formation|32551|6|Mentioned|p101|||U.Sturtian lithology||||||
17814|Tapley Hill Formation|32720|6|Mentioned|p7|||||||||
17814|Tapley Hill Formation|32722|6|Mentioned|Fig.3|||Adelaidean. Stromatolite||||||
17814|Tapley Hill Formation|32723|6|Mentioned|p95|||See also P98||||||
17814|Tapley Hill Formation|32724|4|Described|p509|||See also pp510-512. Sturtian.||||||07-DEC-06
17814|Tapley Hill Formation|32726|6|Mentioned|p187|||Stromatolites||||||
17814|Tapley Hill Formation|32768|6|Mentioned|p49|||Pyritic stratum||||||
17814|Tapley Hill Formation|33224|6|Mentioned|p53|||||||||
17814|Tapley Hill Formation|33336|6|Mentioned|p244|||||||||
17814|Tapley Hill Formation|33422|6|Mentioned|Map legend|Precambrian|Precambrian|||||||
17814|Tapley Hill Formation|33423|4|Described|p13|||||||||
17814|Tapley Hill Formation|33470|6|Mentioned|Table 1|||||||||
17814|Tapley Hill Formation|33474|6|Mentioned|Fig.2|||||||||
17814|Tapley Hill Formation|33726|6|Mentioned|p11|||||||||
17814|Tapley Hill Formation|33957|6|Mentioned|p36|||||||||
17814|Tapley Hill Formation|34011|5|Briefly described|p67|||Petrographic description||||||
17814|Tapley Hill Formation|34175|6|Mentioned|p36|||||||||
17814|Tapley Hill Formation|34176|5|Briefly described|p51|||||||||
17814|Tapley Hill Formation|34202|6|Mentioned|p1057|||See also p1058. Precambrian||||||14-DEC-06
17814|Tapley Hill Formation|34267|6|Mentioned|Fig.|||The Oraparinna and Enorama diapiric structures.||||||14-DEC-06
17814|Tapley Hill Formation|34268|6|Mentioned|p241|||U.Prot.||||||
17814|Tapley Hill Formation|34269|6|Mentioned|Table 1|||||||||
17814|Tapley Hill Formation|34285|4|Described|p178|||Lithology, structure and mineralization.||||||07-DEC-06
17814|Tapley Hill Formation|34291|6|Mentioned|p11|||See also pp12,13. Adelaidean. Equiv. Wockerawirra Dol.||||||14-DEC-06
17814|Tapley Hill Formation|34521|5|Briefly described|p156|||||||||
17814|Tapley Hill Formation|34534|6|Mentioned|Fig.2.13|||||||||
17814|Tapley Hill Formation|34535|5|Briefly described|p66|||||||||
17814|Tapley Hill Formation|34536|6|Mentioned|Map legend|Precambrian|Precambrian|Farina Sup-Gp.Sturtian||||||
17814|Tapley Hill Formation|34587|5|Briefly described|p36|||||||||
17814|Tapley Hill Formation|34766|6|Mentioned|p58|||||||||
17814|Tapley Hill Formation|34812|6|Mentioned|p134|||||||||
17814|Tapley Hill Formation|34833|6|Mentioned|p76|||||||||
17814|Tapley Hill Formation|35002|6|Mentioned|p29|||||||||
17814|Tapley Hill Formation|35075|6|Mentioned|p77|||||||||
17814|Tapley Hill Formation|35135|6|Mentioned|p4|||||||||
17814|Tapley Hill Formation|35217|6|Mentioned|p172|||||||||
17814|Tapley Hill Formation|35255|5|Briefly described|p9|||See also Fig.3.||||||
17814|Tapley Hill Formation|35270|6|Mentioned|p2|||||||||
17814|Tapley Hill Formation|35565|6|Mentioned|p15|||Geochemistry program||||||
17814|Tapley Hill Formation|35582|6|Mentioned|p51|||||||||
17814|Tapley Hill Formation|35628|4|Described|Table 2|||||||||
17814|Tapley Hill Formation|35678|6|Mentioned|Fig.2|||Geological cross-sections, northern Yorke Peninsula.||||||
17814|Tapley Hill Formation|35863|6|Mentioned|p288|||||||||
17814|Tapley Hill Formation|36048|6|Mentioned|p379|||||||||
17814|Tapley Hill Formation|36084|6|Mentioned|Fig.2|||See also P486.||||||
17814|Tapley Hill Formation|36096|6|Mentioned|Fig.3|||||||||
17814|Tapley Hill Formation|36126|6|Mentioned|Fig.1|||See also P1.||||||
17814|Tapley Hill Formation|36137|4|Described|p14|||Palaeomagnetism discussed.||||||
17814|Tapley Hill Formation|36212|5|Briefly described|p3|||||||||
17814|Tapley Hill Formation|36245|6|Mentioned|Fig.1|||||||||
17814|Tapley Hill Formation|36625|6|Mentioned|Fig.1|||||||||
17814|Tapley Hill Formation|36731|6|Mentioned|p124|||||||||
17814|Tapley Hill Formation|36733|4|Described|p51|||||||||
17814|Tapley Hill Formation|36837|6|Mentioned|p50|||||||||
17814|Tapley Hill Formation|36898|6|Mentioned|Fig.4|||||||||
17814|Tapley Hill Formation|36920|6|Mentioned|Table 1|||||||||
17814|Tapley Hill Formation|36952|6|Mentioned|p99|||||||||
17814|Tapley Hill Formation|37238|5|Briefly described|p363|||See also p367.||||||07-DEC-06
17814|Tapley Hill Formation|37371|6|Mentioned|p382|||||||||
17814|Tapley Hill Formation|37461|4|Described|p339|||See also Table 5.I||||||
17814|Tapley Hill Formation|37932|6|Mentioned|p539|||||||||
17814|Tapley Hill Formation|38011|6|Mentioned|p126|||||||||
17814|Tapley Hill Formation|38110|6|Mentioned|p2|||||||||
17814|Tapley Hill Formation|38157|6|Mentioned|Table 1|||||||||
17814|Tapley Hill Formation|38581|4|Described|p254|||||||||
17814|Tapley Hill Formation|38873|4|Described|Table 2|||||||||
17814|Tapley Hill Formation|39344|6|Mentioned|Map legend|Precambrian|Adelaidean|Sturtian to Marinoan||||||
17814|Tapley Hill Formation|39348|6|Mentioned|Map legend|Precambrian|Precambrian|Sturtian||||||
17814|Tapley Hill Formation|39349|6|Mentioned|Map legend|Precambrian|Precambrian|Sturtian||||||
17814|Tapley Hill Formation|39350|6|Mentioned|Map legend|Precambrian|Precambrian|Sturtian||||||
17814|Tapley Hill Formation|39351|6|Mentioned|Map legend|Precambrian|Precambrian|Sturtian||||||
17814|Tapley Hill Formation|39352|6|Mentioned|Map legend|Precambrian|Adelaidean|Sturtian to Marinoan||||||
17814|Tapley Hill Formation|39565|6|Mentioned|p38|||||||||
17814|Tapley Hill Formation|39574|6|Mentioned|p158|||||||||
17814|Tapley Hill Formation|39635|6|Mentioned|Fig.2|||||||||
17814|Tapley Hill Formation|39724|6|Mentioned|p108|||||||||
17814|Tapley Hill Formation|39866|4|Described|p267|||||||||
17814|Tapley Hill Formation|40003|5|Briefly described|Table 15|||See also Table 16||||||
17814|Tapley Hill Formation|40059|6|Mentioned|p6|||||||||
17814|Tapley Hill Formation|40153|6|Mentioned|Plate 2|||||||||
17814|Tapley Hill Formation|40220|6|Mentioned|p7|||||||||
17814|Tapley Hill Formation|40225|4|Described|Map sheet|||||||||
17814|Tapley Hill Formation|40228|5|Briefly described|Fig.1|||||||||
17814|Tapley Hill Formation|40257|6|Mentioned|Fig.2|||||||||
17814|Tapley Hill Formation|40294|3|Fully described|p48|||See also p14.||||||11-DEC-06
17814|Tapley Hill Formation|40442|6|Mentioned|p10|||||||||
17814|Tapley Hill Formation|40445|6|Mentioned|p54|||||||||
17814|Tapley Hill Formation|40448|5|Briefly described|p38|||||||||
17814|Tapley Hill Formation|40453|5|Briefly described|p58|||||||||
17814|Tapley Hill Formation|40456|6|Mentioned|Fig.2|||||||||
17814|Tapley Hill Formation|40503|4|Described|p101|||||||||
17814|Tapley Hill Formation|40763|6|Mentioned|p209|||||||||
17814|Tapley Hill Formation|40852|5|Briefly described|p27|||||||||
17814|Tapley Hill Formation|40856|5|Briefly described|p312|||||||||
17814|Tapley Hill Formation|40910|6|Mentioned|p12|||||||||
17814|Tapley Hill Formation|40911|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
17814|Tapley Hill Formation|40945|6|Mentioned|Fig.3|||||||||
17814|Tapley Hill Formation|41005|6|Mentioned|Fig.2|||||||||
17814|Tapley Hill Formation|41119|6|Mentioned|Fig.2|||||||||
17814|Tapley Hill Formation|41364|5|Briefly described|p165|||||||||
17814|Tapley Hill Formation|41401|6|Mentioned|p34|||||||||
17814|Tapley Hill Formation|41403|6|Mentioned|p49|||||||||
17814|Tapley Hill Formation|41405|3|Fully described|p161|||||||||
17814|Tapley Hill Formation|41493|6|Mentioned|Table 1|||||||||
17814|Tapley Hill Formation|41494|6|Mentioned|p34|||||||||
17814|Tapley Hill Formation|41496|5|Briefly described|Fig.1|||||||||
17814|Tapley Hill Formation|41500|4|Described|p79|||||||||
17814|Tapley Hill Formation|41526|6|Mentioned|p5|||||||||
17814|Tapley Hill Formation|41647|6|Mentioned|p834|||See also Fig.2||||||
17814|Tapley Hill Formation|41667|6|Mentioned|Fig.3|||||||||
17814|Tapley Hill Formation|41770|5|Briefly described|p238|||||||||
17814|Tapley Hill Formation|42087|5|Briefly described|p13|||See also Fig.2||||||
17814|Tapley Hill Formation|42088|5|Briefly described|p544|||See also Fig.2 p546.||||||14-DEC-06
17814|Tapley Hill Formation|42093|5|Briefly described|p6|||See also Fig.2||||||
17814|Tapley Hill Formation|42098|5|Briefly described|p53|||||||||
17814|Tapley Hill Formation|42101|6|Mentioned|p84|||||||||
17814|Tapley Hill Formation|42109|5|Briefly described|p18|||See also Fig.2||||||
17814|Tapley Hill Formation|42167|5|Briefly described|p119|||See also Fig.1||||||
17814|Tapley Hill Formation|42168|6|Mentioned|Fig.3 P123|||||||||
17814|Tapley Hill Formation|42215|5|Briefly described|p451|||||||||
17814|Tapley Hill Formation|42222|5|Briefly described|p16|||||||||
17814|Tapley Hill Formation|42223|6|Mentioned|Table 1 P38|||||||||
17814|Tapley Hill Formation|42235|4|Described|p139|||||||||
17814|Tapley Hill Formation|42238|5|Briefly described|Table 1 P74|||||||||
17814|Tapley Hill Formation|42239|6|Mentioned|Fig.2 P151|||||||||
17814|Tapley Hill Formation|42243|5|Briefly described|p211|||||||||
17814|Tapley Hill Formation|42272|6|Mentioned|p403|||||||||
17814|Tapley Hill Formation|42357|6|Mentioned|p9|||||||||
17814|Tapley Hill Formation|42505|5|Briefly described|Map legend|Adelaidean (Sturtian)|Adelaidean (Sturtian)|||||||
17814|Tapley Hill Formation|42542|5|Briefly described|Fig.2a P11|||||||||
17814|Tapley Hill Formation|42546|5|Briefly described|Map legend|Adelaidean (Marinoan)|Adelaidean (Sturtian)|||||||
17814|Tapley Hill Formation|42720|5|Briefly described|map legend|Sturtian||||||||
17814|Tapley Hill Formation|42723|5|Briefly described|map legend|Sturtian||||||||
17814|Tapley Hill Formation|42736|5|Briefly described|map legend|Neoproterozoic||||||||
17814|Tapley Hill Formation|42779|5|Briefly described|Table 1 P287|||||||||
17814|Tapley Hill Formation|42813|5|Briefly described|p20|||Of the Farina Subgroup.||||||07-DEC-06
17814|Tapley Hill Formation|42882|5|Briefly described|p7, Table 1 p3|||Of the Umberatana Group.||||||07-DEC-06
17814|Tapley Hill Formation|43011|6|Mentioned|Table 2,p12|||||||||
17814|Tapley Hill Formation|43048|4|Described|Table 1.|||||||||
17814|Tapley Hill Formation|43052|4|Described|p186,Table 6.1|||||||||
17814|Tapley Hill Formation|43591|6|Mentioned|p162|||||||||
17814|Tapley Hill Formation|43595|5|Briefly described|p546||Neoproterozoic|(Sturtian)||||||
17814|Tapley Hill Formation|43622|6|Mentioned|p38|Neoproterozoic||||||||
17814|Tapley Hill Formation|43742|6|Mentioned|Fig.2,p39||Neoproterozoic|||||||
17814|Tapley Hill Formation|43845|5|Briefly described|Fig3 p43, 41,42||Neoproterozoic|In Umberatana Group||||||12-JUL-16
17814|Tapley Hill Formation|44133|5|Briefly described|p50, 54|||||||||
17814|Tapley Hill Formation|44659|5|Briefly described|map legend|||Marinoan, lithology.||||||
17814|Tapley Hill Formation|44660|14|Not recorded|map legend|||Sturtian, lithology.||||||
17814|Tapley Hill Formation|44689|14|Not recorded|map legend|||Andamooka. (H53-12).||||||
17814|Tapley Hill Formation|44690|4|Described|map legend|||Geol. Atlas Series. (I/54-5). Includes Tindelpina Member. Sturtian.||||||
17814|Tapley Hill Formation|44934|5|Briefly described|Map Legend||Adelaidean|||||||
17814|Tapley Hill Formation|45155|6|Mentioned|p26|||||||||
17814|Tapley Hill Formation|46865|6|Mentioned|p43|||||||||
17814|Tapley Hill Formation|47004|6|Mentioned|p328|||||||||
17814|Tapley Hill Formation|47012|6|Mentioned|p332|||||||||
17814|Tapley Hill Formation|47020|6|Mentioned|p336|||||||||
17814|Tapley Hill Formation|49792|5|Briefly described|Fig.5|||||||||
17814|Tapley Hill Formation|60718|5|Briefly described|p49 Fig. 2, p53, 55|Adelaidean|Adelaidean|Geol. Prov: Adelaide Geosyncline. See also p51 Fig. 3.||Of Nepouie Subgroup.|Includes Tindelpina Shale Member.|Unconformably underlies Yankaninna and Amberoona Fm. Overlies Boorloo Siltstone. Tindelpina Shale Member gradationally(?) overlies Serle Conglomerate in Breaden Hill area.||15-APR-11
17814|Tapley Hill Formation|60889|6|Mentioned|p251|Neoproterozoic|Neoproterozoic|Traces of gas recorded (Blinman-2).||||||
17814|Tapley Hill Formation|60955|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Of the Umberatana Group. Includes Tindelpina Shale Member. Grey and green laminated siltstones, thin yellow weathering dolomites.||||||13-APR-05
17814|Tapley Hill Formation|60958|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Grey, bedded to laminated shale and dolomitic shale with thin silty dolomite. Sandstone. Geological Province: Adelaide Geosyncline.||||||
17814|Tapley Hill Formation|60959|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Of the Nepouie Subgroup. Finely laminated grey-green siltstone to fine lithic sandstone cycles.||||||29-APR-05
17814|Tapley Hill Formation|61121|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Grey, thin-bedded to laminated shale and dolomitic shale with thin silty dolomite.  Locally thin, fine-grained sandstone. Basal sandstone with rip-up siltstone clasts. Geological Province: Adelaide Geosyncline.||||||
17814|Tapley Hill Formation|61236|6|Mentioned|p24 Fig. 1|Adelaidean|Adelaidean|||||||
17814|Tapley Hill Formation|61237|5|Briefly described|p36|||Produced the Tapley Hill Bluestone, quarried from its siltstone constituent from late 1800s till the 1920s.||||||16-AUG-05
17814|Tapley Hill Formation|61238|4|Described|p46 Fig. 2, p47 Fig. 3|Neoproterozoic|Neoproterozoic|Of the Umberatana Group. Siltstone, grey to black, dolomitic, pyritic and calcareous.||||||
17814|Tapley Hill Formation|61732|5|Briefly described|p25, p132|Sturtian|Sturtian|Of the Nepouie Subgroup (Umberatana Group). Includes Tindelpina Shale and Mount Caernarvon Greywacke Members. Contains Proterozoic microfossils in the shale component. Geological Province: Adelaide Rift Complex.||||||07-FEB-11
17814|Tapley Hill Formation|62085|6|Mentioned|p20 fig 5|Cryogenian|Cryogenian|||Umberatana Group||||
17814|Tapley Hill Formation|62428|5|Briefly described|p351 Tb. 6|Neoproterozoic III|Neoproterozoic III|Age: 750+/-53Ma (Rb-Sr). Palaeomagnetic data.||||||10-FEB-09
17814|Tapley Hill Formation|62592|5|Briefly described|p50 Table 5.1, pp57-58.|Sturtian|Sturtian|Adelaide Geosyncline. Widespread deposition during post-Sturtian-glaciation inundation of the eastern margin of the Gawler Craton.||Unit in Nepouie Subgroup.||Unconformably overlies Yudnamutana Subgroup. Is overlain by Wockerawirra Dolomite.|Siltstone, limestone, dolomite, sandstone.|
17814|Tapley Hill Formation|62664|5|Briefly described|p138 Fig.2, p154.|Neoproterozoic|Neoproterozoic||750 +/- 53 Ma (Preiss 1987)|Unit in Umberatana Group.|||Siltstone, shale, carbonates.|
17814|Tapley Hill Formation|62903|5|Briefly described|p729, p730 Fig.1, p731|Sturtian|Sturtian|Adelaide Rift Complex. Postglacial. Depositional environment was developing passive margin (Preiss 2000). Tindelpina Shale Member at base marks end of Sturtian glaciation. Date from McKirdy et al. 2001.|750+/-53 Ma Rb-Sr whole-rock shale date||Tindelpina Shale Member (at base)|Tindelpina Shale Member (base of Tapley Hill Formation) overlies Yudnamutana Subgroup; relationship with Wockerawirra Dolomite not specified.|dolomitic shales and siltstones|
17814|Tapley Hill Formation|63458|6|Mentioned|p897 Fig.19. |Cryogenian|Cryogenian|||Unit in Umberatana Group.||||
17814|Tapley Hill Formation|64282|5|Briefly described|Map legend|Neoproterozoic III|Neoproterozoic III|Geological Province: Adelaide Geosyncline. Grey, thin bedded to laminated shale and dolomitic shale with thin silty dolomite; locally thin, fine-grained sandstone; basal sandstone with rip-up siltstone clasts; deep marine shelf deposit.||||||
17814|Tapley Hill Formation|64769|6|Mentioned|p27|Neoproterozoic|Neoproterozoic|SA. Willunga Slate dimension stone is from this unit.||||||06-MAY-09
17814|Tapley Hill Formation|64797|5|Briefly described|p151, p153 Fig.2, p159, p162 Fig.9. |||See also p163-166, p167 Tb.10, p168, p169 Fig.12, p170-171, p172 Tb.13, p175. Adelaide Rift Complex. S-isotope data. International correlations.|~700 Ma.|||Correlated with Aralka Formation in Amadeus Basin.||
17814|Tapley Hill Formation|64801|5|Briefly described|p110 Fig.2, p111-112|Neoproterozoic|Neoproterozoic|Adelaide Rift Complex. Deposited during the post-Sturtian glaciation transgression.||Umberatana Group.||Is overlain unconformably by Sunderland Formation.|Deep-water shale and siltstone succession, topped by a shallow-water carbonate unit.|
17814|Tapley Hill Formation|64846|5|Briefly described|p197-209       |Cryogenian|Cryogenian|Carbon isotope details.||Of the Nepouie Subgroup.|Includes Tindelpina Shale, Mount Caernarvon Greywacke, Wockerawirra Dolomite, Members.||Basal shale unit overlain by siltstone unit, cyclic unit, quartz sandstone unit, and transitional shale unit on top.|
17814|Tapley Hill Formation|65375|4|Described|p7, pp25-26.|Neoproterozoic|Neoproterozoic|Sediments deposited along the Torrens Hinge Zone marginal to Adelaide Geosyncline. Deposition probably deep-marine shelf, below storm-wave base. Contains leiosphaeroidal acritarchs.||||Unconformably overlies Sturt Tillite. Unconformably overlain by Winulta Formation.|Grey, thin-bedded to laminated shale and dolomitic shale, with thin silty dolomite layers and local, thin, fine-grained sandstone layers; at the base is sandstone or grainstone with rip-up siltstone clasts.|
17814|Tapley Hill Formation|65376|6|Mentioned|p139.|||153m thick at Emmie Bluff prospect. Contains Cu-Co-Ag mineralisation.||||Overlies Pandurra Formation. Is overlain by Whyalla Sandstone.||
17814|Tapley Hill Formation|65379|5|Briefly described|p643, p644|Neoproterozoic|Neoproterozoic|Of Umberatana Group (Heyson Supergroup). Siltstone, grey to black; dolomite, grey; limestone conglomerate, intraformational; greywacke. N.B. Asbestos deposit host, contains Orroroo asbestos prospect and Mt Rose asbestos occurrence.||||||07-MAR-12
17814|Tapley Hill Formation|65390|5|Briefly described|p18|||Overlies Beda Volcanics. Hosts Kupferschiefer-type Myall Creek copper mineralisation near its base.||||||
17814|Tapley Hill Formation|65493|4|Described|p907-24, Fig 1-6,10,12-16|Cryogenian|Cryogenian|Of Nepouie Subgroup. Includes Tindelpina Shale Member. Underlies the Balcanoona Formation. Conformably and disconformably overlies Merinjina Tillite. Max thickness 550m. Dominantly deep water deposition.||||||
17814|Tapley Hill Formation|65892|5|Briefly described|p33 Fig.18.|Cryogenian|Cryogenian|||Unit in Umberatana Group.||Overlies Wilyerpa Formation. Is overlain by Sunderland Formation.||
17814|Tapley Hill Formation|65925|5|Briefly described|p124 Fig.3, Appendix 2.|||||Unit in Umberatana Group.|||Siltstone, grey to black, dolomitic and pyritic grading upwards to calcareous, thinly laminated, locally crossbedded; dolomite, grey, flaggy to massive; limestone conglomerate, intraformational; greywacke.|
17814|Tapley Hill Formation|67030|6|Mentioned|p408, p409 Fig. 2|Cryogenian|Cryogenian|||Farina Subgroup|Includes Tindelpena Shale Member.|Overlies the Wilyerpa Formation, Sturt Tillite and Appila Tillite; underlies and laterally equivalent to the Brighton Limestone and Tarcowie Siltstone.||26-APR-12
17814|Tapley Hill Formation|67180|4|Described|p600-602, p606, p610, Figs. 1-4, 6, 10|Cryogenian|Cryogenian|Sturtian Age. Overlies the Sturtian glacials. Informal units: Siltstone Unit, Cyclic Unit, Quartz-Sandstone Unit, Transitional Shale Unit (Giddings et al. 2009); these occur above the Tindelpina Shale Member.||Unit in Nepouie Subgroup|Includes Tindelpina Shale Member|Unconformably underlies the Yankaninna Formation; gradational contact with overlying Balcanoona Formation or partial lateral equivalent; overlies the Merinjina Tillite.|Deep-water shales, interbedded laminated dolomites and shales, calcareous siltstones and shales, quartz-sandstone, turbiditic beds, carbonate beds.|
17814|Tapley Hill Formation|67484|6|Mentioned|p294 Tb.1|Cryogenian|Cryogenian|Adelaide Rift Complex.||Of the Umberatana Group.||Overlain by the Elatina Formation. Underlain by the Sturtian Tillite.||
17814|Tapley Hill Formation|67620|5|Briefly described|p5|Cryogenian|Cryogenian|Adelaide Rift Complex.||Umberatana Group.||Overlies Sturtian Tillite. Is overlain by Elatina Formation.||
17814|Tapley Hill Formation|67856|6|Mentioned|p344|Neoproterozoic|Neoproterozoic|SA.|750 +/-53 Ma|||||
17814|Tapley Hill Formation|67870|5|Briefly described|p9, p31|Neoproterozoic|Neoproterozoic|Adelaide Rift System.||Nepouie Subgroup.|Tindelpina Shale Member.|||
17814|Tapley Hill Formation|67979|4|Described|p529-532,536-539, Figs.1-10, p541-545|Sturtian||Variability of unit in different sections is described. Tindelpina Shale Member common to all. Age from the lower Tapley Hill Formation supported by underlying Sturtian glacigenic successions (Kendall et al. 2006). Previously included Willigan Member at top, now considered very localised, lower member of Yankaninna Formation (herein). Previously included Wockerawirra Dolomite Member (now overlies Tapley Hill Formation).|643+/-2.4 Ma, Re-Os age, (Kendall et al. 2006)|Nepouie Subgroup|Tindelpina Shale Member, Serle Conglomerate Member base, Mount Caernarvon Greywacke Member.|Overlies Merinjina Tillite, Bolla Bollana Fmn; angular unconf. over Lyndhurst Fmn. Overlain by Yankaninna Fmn, sedimentary breccia (Tindelpina area) or erosionally overlain by Wockerawirra Dolomite .|Interglacial, deep marine unit. Siltstone, shale, quartz-sandstone, conglomerate, dolomite, limestone and turbidite beds|22-SEP-14
17814|Tapley Hill Formation|68030|6|Mentioned|p236, p238|||Flinders Ranges. Interglacial deposit.||Unit of Umberatana Group.|Includes Tindelpina Shale Member.|||26-JUN-19
17814|Tapley Hill Formation|68126|5|Briefly described|p31|Neoproterozoic|Neoproterozoic||||||Siltstone, grey to black, dolomitic and pyritic grading up to calcareous.|
17814|Tapley Hill Formation|68131|6|Mentioned|p89|Neoproterozoic|Neoproterozoic|||||||
17814|Tapley Hill Formation|68138|6|Mentioned|p156|Neoproterozoic|Neoproterozoic|Adelaide Rift Complex.||Umberatana Group.||||
17814|Tapley Hill Formation|68275|6|Mentioned|p56, 58, 62|||Associated with the Aralka Formation in that they both show sustained and very high positive 34S (pyrite) isotope anomalies; a unique chronostratigraphic marker.||||||
17814|Tapley Hill Formation|68473|6|Mentioned|p531|||Adelaide Rift Complex.||||||
17814|Tapley Hill Formation|69019|4|Described|p40, p46-48, p162-163.|Neoproterozoic|Neoproterozoic|Of Coats (in Thomson et al. 1964). Regionally extensive throughout Adelaide Geosyncline. Thickness from <200 m to >500 m. Age from Re-Os analysis of organic matter.|643 +/- 2.4 Ma (Kendall et al. 2006).||Includes Tindelpina Shale Member.|Unconformably overlies Wilyerpa Formation and Skillogalee Dolomite. Conformably overlies Serle Conglomerate.|Grey to black, thinly laminated siltstone; variable carbonate cement, pyrite, and carbonaceous matter; grades upwards into calcareous siltstone with dolomite, limestone conglomerate and greywacke.|
17814|Tapley Hill Formation|69023|5|Briefly described|p67|||Stuart Shelf. Stratigraphically below Balcanoona Formation. Maximum isochron age: Webb and Coats, 1980; Preiss et al, 1998.|750 +/- 63 Ma (Rb-Sr whole rock).|||||
17814|Tapley Hill Formation|69438|6|Mentioned|p23:16|||Adelaide Fold Belt.||||Is correlated with the Aralka Formation (Amadeus Basin).||12-JUL-16
17814|Tapley Hill Formation|69666|5|Briefly described|p26, p28, p31, p33, p39|Neoproterozoic|Neoproterozoic|Early Sturtian.|||Tindelpina Shale Member.|Unconformably overlies Beda Basalt.||
17814|Tapley Hill Formation|69841|5|Briefly described|p21|||Adelaide Geosyncline. Has somewhat similar lithology to Robbins Creek Formation (King Island).|Between 659 and 635 Ma (Grey et al., 2011).|||||
17814|Tapley Hill Formation|70021|5|Briefly described|p97-98|Neoproterozoic|Neoproterozoic|Deposition was synchronous with Oodnaminta Reef Complex.||||Contains debris from Oodnaminta Reef Complex (Balcanoona Formation).|Basinal shales. Contains large quantities of allochthonous reef debris (as debris flows).|
17814|Tapley Hill Formation|70031|4|Described|p245-246,248,250|Cryogenian|Cryogenian|Adelaide Geosyncline. Lower interglacial succession; waning stages of Sturtian glaciation. Thickness: 2400m. A widespread unit recording post-glacial eustatic rise of sea-level with marine transgression extending onto the Stuart Shelf and Gawler Craton (Preiss 1987b; Coats and Preiss 1987; Preiss et al. 2011). Ca. 650 Ma date for late Cryogenian to post-Delamerian Orogeny poles. See p250 Table 2 for paleomagnetic analysis.||Unit of Nepouie Subgroup.|Includes Tindelpina Shale Member.|Overlain by Brighton Limestone. Underlain conformably by Tindelpina Shale Member.|Dark bluish grey, slightly calcareous or dolomitic, locally pyritic, laminated siltstone.|
17814|Tapley Hill Formation|70082|5|Briefly described|p2-3|Cryogenian|Cryogenian|Flinders Ranges, Stuart Shelf and Kulpara-Adelaide region.|||Includes Tindelpina Shale Member and Woocalla Dolomite Member.|Overlain unconformably by Wilmington and Angepena formations.||
17814|Tapley Hill Formation|70323|5|Briefly described|p212-213|Cryogenian|Cryogenian|Central Flinders Ranges, Adelaide Geosyncline. Associated with Sturtian glaciation, but specifically represents the beginning of interglacial period after peak Sturtian glaciation.|c. 650 Ma|Unit of Nepouie Subgroup.||Underlain by Wilyerpa Formation/Yudnamutana Subgroup.|Non-lonestone-bearing siltstones and shales.|
17814|Tapley Hill Formation|70333|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic||||||Siltstone, grey to black, dolomitic and pyritic grading upwards to calcareous, thinly laminated, locally cross-bedded; dolomite, grey, flaggy to massive; limestone conglomerate, intraformational; greywacke.|
17814|Tapley Hill Formation|70334|4|Described|p2,8,20-22,38-39,47-55,60,77,83,87-90,92|Neoproterozoic|Neoproterozoic|Geological province: Gawler Craton. Of Adelaide Geosyncline and Stuart Shelf. Thickness: 15-150m on CULTANA, thinning westward. Part of a transgressive-regressive sequence with the Brighton Limestone, following Sturtian glacial maximum and eustatic sea level rise from melting of extensive ice sheets and first marine incursion and sedimentation on the Gawler Craton. Probable deep basinal setting based on lateral persistance and high organic carbon content. Likely derived from Gawler Craton, consistent with paleocurrent indicators (Preiss 1973, Preiss 1987). Onlaps onto eastern edge of North Whaylla Hills, which comprises basement highs of the underlying Beda Basalt, Backy Point Formation and Pandurra Formation.||Unit of Nepouie Subgroup.|Includes Tassie and Lincoln members.|Overlain by Brighton Limestone or unconformably by the Whyalla Sandstone or Wilmington Formation. Underlain unconformably by Beda Basalt or Backy Point Formation or Pandurra Formation.|Grey-green finely-laminated calcareous and dolomitic siltstone with minor grey-green fine-grained laminated sandstone interbeds, becoming more calcareous toward upper parts of the formation.|14-OCT-19
17814|Tapley Hill Formation|70384|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Adelaide Geosyncline. The lenticular conglomerate is separately mapped, and consists of sandy dolomitic matrix and grit to boulder sized erratics of the lower part of the Formation and underlying Yudnamutana Subgroup. The upper section contains fallen blocks of Balcanoona Formation from the reef-front. Age shown more specifically as Sturtian [Cryogenian].||Of Nepouie Subgroup.|Includes Tindelpina Shale Member.|Overlies Serle Conglomerate. Is overlain unconformably by Balcanoona Formation.|Grey to black, dolomitic, pyritic siltstone, thinly laminated, locally cross-bedded, grades upwards to calcareous siltstone; grey, flaggy to massive dolomite; intraformational limestone conglomerate and greywacke; lenticular conglomerate.|23-JAN-19
17814|Tapley Hill Formation|70407|5|Briefly described|p103 Fig 2, p112|Neoproterozoic|Neoproterozoic|Age: Sturtian.||Of Umberatana Group.|Includes Wockerawirra Dolomite Member, Sunderland Member, Mount Caernarvon Greywacke Member.|Unconformably overlain by Tarcowie Siltstone.||
17814|Tapley Hill Formation|70659|6|Mentioned|p10|Neoproterozoic|Neoproterozoic|||||||
17814|Tapley Hill Formation|70816|6|Mentioned|p3|Neoproterozoic|Neoproterozoic|Gawler Ranges region.||||||
17814|Tapley Hill Formation|70819|5|Briefly described|p11, 13, 29, 31|Neoproterozoic|Neoproterozoic|Clare Valley. Youngest preserved rocks of the Adelaide Geosyncline in the area. Relatively deep-marine shelf environment. Generally poorly exposed; occupies the Polish Hill River Valley.|643 +/- 2.4 Ma (Re-Os).|Nepouie Subgroup.|Tindelpina Shale Member.|Overlies Wilyerpa Formation.|Carbonaceous siltstones.|
17814|Tapley Hill Formation|70948|6|Mentioned|p974|Neoproterozoic|Neoproterozoic|Geological province: Gawler Craton.||||||
17814|Tapley Hill Formation|71037|5|Briefly described|p22-23 Fig.2, p27 Fig.6|Neoproterozoic|Neoproterozoic|Shown only on the Six Mile Hill 1:75,000 surface geology map and the interpreted bedrock geology diagram p27 Fig.6. Age shown as Sturtian.||Umberatana Group||Shown as older than Upalinna and Yerelina Subgroups.|Grey to black, laminated siltstone, dolomitic and pyritic; intra-formational conglomerate.|
17814|Tapley Hill Formation|71129|4|Described|p1,15-16,64,89,98,101-102,105|Sturtian|Sturtian|Of Stuart Shelf. Records first marine transgression of the Stuart Shelf after Sturt Glaciation. Consists of a transgressive-regressive sequence of mainly carbonaceous and dolomitic siltstones and shales deposited during the late Sturtian Epoch. Regionally extensive in the subsurface. Outcrops are limited to a few exposures around the Pandurra Homestead; the best exposures occur in a recently excavated dam about 1km to the west of the homestead. Locally overlain by a coarse-grained basal conglomeratic unit which may equate to Moonlight Conglomerate or possible correlatives. Maximum thickness in SIX MILE HILL is 224m (intersected in PACMINEX EX 163 drillhole 140303), also intersected 173m thick interval in NSDP02 drillhole 287996. Initially deposited adjacent basement highs; dominantly within fluvial to nearshore marine environments. Uppermost part of the unit displays extensive evidence of shallowing e.g. increasing carbonate and silt content, scouring and ripple cross-lamination. Geochronological results include siltstone Rb-Sr whole rock isochron age of 750+\-63 Ma (Webb and Coats, 1980), interpreted to be max depositional age (Preiss et al., 1998). Also contains Re-Os age of 643+\-2.5 Ma of organic matter from Tindelpina Shale Member. See also p107-112,114,116,126-127,184,187,208,210,225,227.|643+\-2.4 Ma (Re-Os)|Unit of Nepouie Subgroup.|Includes El Alamein, Tassie and Lincoln members, Magazine Hill Clay and the Tindelpina Shale Member.|Overlain by Augusta Shale or Moonlight Conglomerate. Underlain by Beda Basalt or Backy Point Formation or Gawler Range Volcanics or Pandurra Formation.|Grey, laminated, dolomitic and carbonaceous shales and siltstones.; highly weathered in outcrop. Elsewhere consists of whitish to light brown, highly weathered, laminated kaolinitic shales and mudstones.|13-NOV-19
17814|Tapley Hill Formation|71130|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Age shown as Sturtian.||Umberatana Group.|||Grey to black laminated siltstone, dolomitic and pyritic, intra-formational conglomerate.|
17814|Tapley Hill Formation|71131|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Age shown as Sturtian.||Umberatana Group.|||Grey to black laminated siltstone, dolomitic and pyritic, intra-formational conglomerate.|
17814|Tapley Hill Formation|71235|6|Mentioned|p5|Neoproterozoic|Neoproterozoic|||||||
17814|Tapley Hill Formation|71236|6|Mentioned|p28-p29|Cryogenian|Cryogenian|[Probably overturned, given that it is older than the underlying Beda Volcanics].|750 +/- 53 Ma (Rb-Sr, Webb and Coats, 1980)|||Unconformably overlies the Beda Volcanics.||
17814|Tapley Hill Formation|71237|2|Defined|p7, 8, 10, 11, 18|||||||||
17814|Tapley Hill Formation|71712|5|Briefly described|p411, p415, 419|Neoproterozoic|Neoproterozoic|Represents marine incursion of the eastern Gawler Craton following Sturtian glaciation.|Re-Os age 643+/-2 Ma near base.|Unit of Umberatana or Wilpena groups.||Overlies Pandurra Formation.||
17814|Tapley Hill Formation|71895|4|Described|p10,  p22, p90, APP4. p4,|||Stuart Shelf. The transition to the Brighton Limestone represents shallowing marine conditions. Spectral analysis is provided. This unit is regionally anomalous in base metals.||Basal Umberatana Group||Conformably (gradationally) overlain by the Brighton Limestone.|Pyritic and carbonaceous, with thinly laminated, dolomite interbeds and lenses.|
17814|Tapley Hill Formation|72090|5|Briefly described|p12, p31, p34-p37, p107-p108|||Gawler Craton. The target of the majority of drilling in the Carriewerloo area was sediment hosted copper within this unit. Calcite veins are common.||||Overlies the Beda Basalt.|Black shales and dolomitic siltstones.|
17814|Tapley Hill Formation|72247|5|Briefly described|p41,43|Neoproterozoic|Neoproterozoic|Of Adelaide Geosyncline.||||Overlain by Whyalla Sandstone.||
17814|Tapley Hill Formation|72429|5|Briefly described|p952, p958|Sturtian|Sturtian|Mount Chambers Gorge, eastern Flinders Ranges.||Umberatana Group||Disconformably underlies the Wockerawirra Dolomite.||
17814|Tapley Hill Formation|72449|5|Briefly described|p1, p2 Map Legend|Neoproterozoic|Neoproterozoic|Includes deep sea muds. Shown as part of diapir formation diagram, p1.||||Overlies Wilyerpa Formation and underlies Sunderland Formation.|Dolomitic siltstone and limestone at top. Dark grey, finely laminated siltstone to fine sandstone cycles . Ridge-forming, fine grained grey-green sandstone. Conglomeratic bands at base around Oraparinna Diapir.|
17814|Tapley Hill Formation|72450|5|Briefly described|Brochure, Brochure map|||Seen primarily in road cuts on the Main South Road, Tapley Hill, Ocean Boulevard and on Willunga Scarp. Deposited in shelf seas during a warmer period. Deformed by the Delamerian Orogeny.||Umberatana Group|||Calcareous siltstone and sandstone; intraclastic and stromatolitic limestone.|
17814|Tapley Hill Formation|72456|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Marree 1:250k map sheet.|||||Siltstone, grey to black, dolomitic to pyritic grading upwards to calcareous, thinly laminated, locally corss-bedded; dolomite, grey, flaggy to massive, limestone conglomerate, intraformational, greywacke.|14-JUN-22
17814|Tapley Hill Formation|72473|6|Mentioned|p4-5||||||Tindelpina Shale Member|||
17814|Tapley Hill Formation|72601|6|Mentioned|p5-6, p8|||||Umberatana Group|Tindelpina Shale Member, Wockerawirra Member|||
17814|Tapley Hill Formation|72613|6|Mentioned|p2 fig 1, p3, p5, p11|Cryogenian|Cryogenian|Shown as Sturtian age. Northern Flinders Ranges.||Umberatana Group|Includes the Tindelpina Shale Member.|Conformably overlies the Yudnamutana Subgroup. Conformably overlain by and laterally equivalent to Balcanoona Formation.|Basinal blue dolomitic shales.|
17814|Tapley Hill Formation|73086|6|Mentioned|p72, p161|||Adelaide Rift Complex.||Umbertana Subgroup, Heysen Supergroup|Wockerwirra Member|Conformably overlain by Brighton Limestone. Correlates to Aralka Formation.||
17814|Tapley Hill Formation|73093|5|Briefly described|map legend|Neoproterozoic|Neoproterozoic||||||Siltstone, grey to black, dolomitic and pyritic dolomite, grey, flaggy to massive partly intraclastic, greywacke.|09-DEC-21
17814|Tapley Hill Formation|73107|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Adelaide Geosyncline.|||||Grey, thin-bedded to laminated shale and dolomitic shale with thin silty dolomite. Locally thin, fine-grained sandstone. Basal sandstone with rip-up siltstone clasts. Deep marine shelf deposit. Acritarchs.|
17814|Tapley Hill Formation|73110|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic||||Tindenpina Shale Member.||Siltstone, grey to black, dolomitic and pyritic grading upwards to calcareous, thinly laminated, locally cross-bedded; dolomite, grey, flaggy to massive; limestone conglomerate, intraformational; greywacke.|
17814|Tapley Hill Formation|73188|5|Briefly described|p315-316, p325-326, p330|Neoproterozoic|Neoproterozoic|Mount Lofty Ranges. Represents the first significant transgression onto the Gawler Craton. Disconformably underlain by glaciomarine and fluvioglacial sediments.||Nepouie Subgroup, Umberatana Group||[Conformably] overlain by Brighton Limestone.|Carbonaceous, calcareous siltstone.|
17814|Tapley Hill Formation|73226|6|Mentioned|p3-4|||||||Underlain by Beda Basalt.|Includes light grey dolomite clast conglomerates within dark grey siltstone and intercalated dark grey and light grey dolomitic siltstones to very fine grained sandstone. Lower portion may include disseminated pyrite within laminated siltstones.|
17814|Tapley Hill Formation|73227|4|Described|p24-26, p29, p35-36|Cryogenian|Cryogenian|Stuart Shelf and Adelaide Rift Complex. Sturtian. In the latter area, a significant post-glacial disconformity at the base of the unit. Possible metal-rich source rock. Contains black shale hosted copper sulfide deposits.|< 663.03 +/- 0.11 Ma U-Pb, < 643 +/- 2.4 Ma Re-Os|Umberatana Group||Underlain by Beda Basalt, Backy Point Formation, Pandurra Formation, and Wilyerpa Formation. Overlain by Brighton Limestone, Yudnapinna beds, and Whyalla Sandstone.|Grey to black dolomitic and pyritic, finely laminated siltstone and dolomite.|
17814|Tapley Hill Formation|73234|5|Briefly described|p6|Cryogenian|Cryogenian||c. 650 Ma|Umberatana Group|||Carbonaceous-dolomitic siltstone and carbonate[?] rocks.|
17814|Tapley Hill Formation|73236|4|Described|p36, p38, p47|Cryogenian|Cryogenian|Marine shelf sedimentary rocks. Occurs only as glacial erratics in Hallett Cove map area. Late Sturtian; represents post-glacial transgression. Deposition under conditions of post-rift thermal subsidence.|c. 660-645 Ma|Nepouie Subgroup, Umberatana Group, Heysen Supergroup||Underlain by Sturt Tillite (Yudnamutana Subgroup). Overlain by Brighton Limestone.|Dark grey thinly laminated calcareous and carbonaceous siltstone with intraclastic limestone lenses near top.|
17814|Tapley Hill Formation|74367|5|Briefly described|p7-9, p11, p14-16, p19-24|Cryogenian|Cryogenian|Previous Rb-Sr whole rock isochron age of 750+/-53 Ma (Webb and Coats, 1980), now considered innacurate.|654+/-13 Ma LA-ICP-MS detrital zircon MDA|Nepouie Subgroup|Tindelpina Shale Member|Overlies Beda Basalt||
17845|Tarcoola Formation|22613|6|Mentioned|p10|||||||||
17845|Tarcoola Formation|22629|4|Described|fig1p146,157,158|Mesoproterozoic|Proterozoic|>2000m thick.||||||23-DEC-08
17845|Tarcoola Formation|23124|5|Briefly described|p395 Fig.1, p397|||||||||
17845|Tarcoola Formation|23481|5|Briefly described|p19 Fig 1|||Geological Province: Gawler Craton.||||||
17845|Tarcoola Formation|23490|6|Mentioned|p22|||||||||
17845|Tarcoola Formation|23805|5|Briefly described|p4 Fig. 1|Paleoproterozoic|Paleoproterozoic|Geological Province: Gawler Craton.||||||07-NOV-08
17845|Tarcoola Formation|24261|5|Briefly described|p1047 Fig.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Gawler Craton||||||
17845|Tarcoola Formation|24422|5|Briefly described|p84 Fig. 1, p107|Paleoproterozoic|Paleoproterozoic|Age: ca. 1655 Ma. Geological Province: Gawler Craton.||||||07-NOV-08
17845|Tarcoola Formation|24472|5|Briefly described|p5 Tb.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Harris Greenstone Domain, Gawler Craton.||||||07-NOV-08
17845|Tarcoola Formation|24505|5|Briefly described|p5 Fig. 1, p7|Paleoproterozoic|Paleoproterozoic|Age: ~1650Ma. Geological Province: Gawler Craton.||||||07-NOV-08
17845|Tarcoola Formation|24597|5|Briefly described|p526 Fig. 1|Paleoproterozoic|Paleoproterozoic|Age: ca1650Ma.  Geological Province: Gawler Craton.  See also p528 Fig. 3, p538.||||||07-NOV-08
17845|Tarcoola Formation|33557|6|Mentioned|p18|||Refers Whitten (1966). Mineralization||||||
17845|Tarcoola Formation|39802|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
17845|Tarcoola Formation|39905|5|Briefly described|p3|||||||||
17845|Tarcoola Formation|40644|6|Mentioned|p121|||Intracontinental, shallow water sequence.||||||13-AUG-08
17845|Tarcoola Formation|40910|6|Mentioned|p11|||||||||
17845|Tarcoola Formation|41402|6|Mentioned|p35|||||||||
17845|Tarcoola Formation|41493|6|Mentioned|Table 1|||||||||
17845|Tarcoola Formation|41609|6|Mentioned|Fig.1|||||||||
17845|Tarcoola Formation|41972|6|Mentioned|Fig.3 P366|||||||||
17845|Tarcoola Formation|41995|5|Briefly described|p12|||||||||
17845|Tarcoola Formation|42167|6|Mentioned|Fig.4 P117|||||||||
17845|Tarcoola Formation|42357|6|Mentioned|p8|||1650Ma||||||
17845|Tarcoola Formation|42465|5|Briefly described|Map Legend|||||||||
17845|Tarcoola Formation|42469|3|Fully described|p13|||||||||
17845|Tarcoola Formation|42536|6|Mentioned|p3|||Kingoonya bedrock drilling||||||
17845|Tarcoola Formation|42546|5|Briefly described|Map legend|Mesoproterozoic||||||||
17845|Tarcoola Formation|42736|5|Briefly described|map legend|Mesoproterozoic||||||||
17845|Tarcoola Formation|43052|4|Described|p68|||||||||
17845|Tarcoola Formation|43053|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Quartzite, shale, conglomerate, minor volcanics.||||||07-NOV-08
17845|Tarcoola Formation|43258|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
17845|Tarcoola Formation|43298|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
17845|Tarcoola Formation|43561|6|Mentioned|p1438|||Age: 1655 Ma.of deposition||||||
17845|Tarcoola Formation|43595|5|Briefly described|p443|||||||||
17845|Tarcoola Formation|43634|6|Mentioned|p13|||||||||
17845|Tarcoola Formation|44935|5|Briefly described|Map Legend||Proterozoic|||||||
17845|Tarcoola Formation|50605|5|Briefly described|p8.3|||Intruded by the Hiltaba Supersuite. Geological Province: Gawler Craton and Curnamona Province.||||||18-JAN-07
17845|Tarcoola Formation|60515|6|Mentioned|p116 Fig.1 |||||||||
17845|Tarcoola Formation|60704|5|Briefly described|p686 Fig.1|Paleoproterozoic|Paleoproterozoic|Includes 3 members: the basal Peela Conglomerate, Fabian Quartzite and Sullivan Shale Members. Geological Province: Gawler Craton.||||||07-NOV-08
17845|Tarcoola Formation|60953|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Age: 1656Ma. Quartzite, shale, conglomerate, minor volcanics.||||||07-NOV-08
17845|Tarcoola Formation|60954|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Geological Province: Gawler Craton.||||||31-MAY-05
17845|Tarcoola Formation|61108|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|Quartzite, shale, conglomerate and minor tuff. Age: 1656 Ma.||||||07-NOV-08
17845|Tarcoola Formation|61262|5|Briefly described|p455 Fig. 11|Paleoproterozoic|Paleoproterozoic|Age: >1650Ma. Geological Province: eastern Gawler Craton.||||||07-NOV-08
17845|Tarcoola Formation|61522|5|Briefly described|p5 Fig.1|||Geological Province: Gawler Craton.||||||
17845|Tarcoola Formation|61864|6|Mentioned|p16 fig 3|||||||||
17845|Tarcoola Formation|63067|5|Briefly described|p2 Fig. 1|Paleoproterozoic|Paleoproterozoic|Age: ~1650Ma. Siltstone, shale, quartzite, conglomerate, tuff, basalt.||||||07-NOV-08
17845|Tarcoola Formation|63276|5|Briefly described|p3 Fig. 2, p14 Fig. 3|Paleoproterozoic|Proterozoic|Comprises Peela Conglomerate, Fabian Quartzite and Sullivan Shale Members. Unconformable over Paxton Granite. Age: ~1656+/-7Ma. Basal conglomerate, arkosic grit with some BIF, upwards into quartzite with carbonate horizons + quartzite and siltstones.||||||07-NOV-08
17845|Tarcoola Formation|63866|5|Briefly described|p6, p9, p17, p30|Statherian|Statherian|Wilgena Domain, Gawler Craton.|c. 1655 Ma (U-Pb zircon)|||Overlies the Wilgena Hill Jaspilite.||
17845|Tarcoola Formation|64130|5|Briefly described|p1378 Fig.1, p1380 Fig.2, p1382, p1387 |Mesoproterozoic|Mesoproterozoic|Thickness >2,000 m.|ca. 1656 Ma (Daly et al., 1998; Budd, 2006)||||Package of clastic sediments, dolomites, dacitic to andesitic volcaniclastic rocks, and carbonaceous shales.|
17845|Tarcoola Formation|64137|5|Briefly described|p1541-1547, p1549 Fig.6, p1552-1555   |Paleoproterozoic|Paleoproterozoic|Hosts Tarcoola goldfield. Neodymium and lead isotope data.|||Includes the Sullivan Shale Member, Fabian Quartzite Member and the Peela Conglomerate Member.|Overlies Paxton Granite . Is intruded by dykes of Lady Jane Diorite.|Metasedimentary rocks.|
17845|Tarcoola Formation|64576|6|Mentioned|p624|||Age: 1650Ma.||||||
17845|Tarcoola Formation|64722|6|Mentioned|p14|Statherian|Statherian|Age not clear. It has been suggested deposition was synchronous with the Ooldean Event (1660-1630 Ma).||||||
17845|Tarcoola Formation|64725|6|Mentioned|p58 Fig.2. |||Gawler Craton.||||||
17845|Tarcoola Formation|64726|6|Mentioned|p83 Fig.2.|||||||||
17845|Tarcoola Formation|64739|6|Mentioned|p264 Fig.1.|||Gawler Craton.||||||
17845|Tarcoola Formation|64828|5|Briefly described|p1064 Fig. 1|Mesoproterozoic|Paleoproterozoic|Geological province: Gawler Craton.||||||04-MAR-09
17845|Tarcoola Formation|65220|5|Briefly described|p20|Paleoproterozoic|Paleoproterozoic|age c.1650||||||10-DEC-09
17845|Tarcoola Formation|65375|6|Mentioned|p13.|Paleoproterozoic|Paleoproterozoic||1657 Ma.|||||
17845|Tarcoola Formation|65376|6|Mentioned|p8 Fig.1.1, pp215-217. |Paleoproterozoic|Paleoproterozoic|||||||
17845|Tarcoola Formation|65385|5|Briefly described|pS128 Fig. 2||Statherian|Gawler Craton. Shale interlayered with rhyodacite-basalt, quartzite and conglomerate. 1656 +/-7 Ma.||||||08-MAR-12
17845|Tarcoola Formation|65390|5|Briefly described|p11 Fig.1, p17, p22 Fig. 3, p26 Tb. 1|Statherian|Statherian|Wilgena Domain, Gawler Craton. Age of about 1660 - 1630 Ma inferred in Figure 3. Intruded by Hiltaba Suite. Gold is found in quartz veins in carbonaceous siltstone and interbedded quartzite.||||||
17845|Tarcoola Formation|65485|6|Mentioned|Fig 1|Paleoproterozoic|Paleoproterozoic|||||||19-MAR-12
17845|Tarcoola Formation|65922|6|Mentioned|p13 Fig. 4|||Gawler Craton.||||||
17845|Tarcoola Formation|66302|6|Mentioned|p4 Fig.3, p19, p21, p23, p32, p34|Statherian|Statherian|Wilgena and Harris Greenstone Domains, Gawler Craton. 800m thick upwards fining succession. See also p76 Fig.20.|ca. 1660 Ma||Includes the Peela Conglomerate, Fabian Quartzite Member and the Sullivan Shale Member.|||
17845|Tarcoola Formation|67058|4|Described|p476, pp479-484, p491, pp496-497.|Paleoproterozoic|Paleoproterozoic|Central Gawler Craton. Its geochemistry is discussed in detail. Maximum zircon U-Pb depositional ages were found (this study) to be 1700 +/- 15 Ma and 1732 +/- 20 Ma. Probable source regions are the Tunkillia Suite, or the Warumpi Province of the North Australian Craton.|1656 +/- 7 Ma (Daly 1993b).||Includes Peela Conglomerate, Fabian Quartzite, Sullivan Shale Member.|Overlies Paxton Granite.||15-MAR-12
17845|Tarcoola Formation|67323|5|Briefly described|Eastern Australia Time-Space Plot; p35|Paleoproterozoic|Paleoproterozoic|Gawler Craton. Fluvial to marginal marine deposits.|1656 +/- 7 Ma.||||Shale, intercalated with rhyolite to basalt, quartzite and conglomerate.|
17845|Tarcoola Formation|67536|5|Briefly described|Map Legend|Statherian|Statherian|Gawler Craton.|1656 +/- 7 Ma.||||Quartzite, shale, conglomerate and minor tuff.|
17845|Tarcoola Formation|67900|5|Briefly described|p20|Paleoproterozoic|Paleoproterozoic|Central Gawler Craton. Post-Kimban Orogeny sedimentation.|c.1657 Ma (Daly et al., 1998).||||Associated with minor mafic magmatism.|
17845|Tarcoola Formation|68128|5|Briefly described|p53|Palaeoproterozoic|Palaeoproterozoic|Gawler Craton.|||||Quartzite interbedded with laminated carbonaceous and pyritic siltstone and shale.|
17845|Tarcoola Formation|68131|5|Briefly described|p2 Fig.1|Paleoproterozoic|Paleoproterozoic||||||Included in a polygon of quartzite, sandstone, shale, conglomerate and minor felsic volcanics.|
17845|Tarcoola Formation|69004|6|Mentioned|p18|||Gawler Craton.||||||
17845|Tarcoola Formation|69591|6|Mentioned|p108 Fig.2.104|||Appears in a diagram of the geodynamic setting of ~1670-1645 Ma eastern Australia.|~1650 Ma.|||||
17845|Tarcoola Formation|69649|6|Mentioned|p6 Fig.4, p49|||Target for Cu exploration.||||||
17845|Tarcoola Formation|70778|6|Mentioned|p24|Statherian|Statherian|Central Gawler Craton.|||Includes the Sullivan Shale Member.|||
17845|Tarcoola Formation|70789|5|Briefly described|p316|||Fault-bound basin deposits.|c.1650 Ma.|||Overlies Mulgathing Complex.|Clastic sedimentary and associated mafic volcanic rocks.|
17845|Tarcoola Formation|70858|6|Mentioned|p14, 31, 32 Figs.15C-D, p33-34|Paleoproterozoic|Paleoproterozoic|Gawler Craton. Similar Zr geochronology and Nd isotope ratios suggest a shared depositional system with Willyama and Isa Supergroups, and the Wernecke Supergroup of Yukon.||||||
17845|Tarcoola Formation|71235|6|Mentioned|p26||||1656+/-7 Ma (Daly et al., 1998)|||||
17845|Tarcoola Formation|71341|6|Mentioned|p188 fig 7|||||||||
17845|Tarcoola Formation|71348|6|Mentioned|p201|Statherian|Statherian|Geological province: Gawler Craton.||||||
17845|Tarcoola Formation|71534|5|Briefly described|p296|||Geological province: Gawler Craton. Deposited into graben in the central region of the Gawler Craton after the Kimban Orogeny.||||||
17845|Tarcoola Formation|71712|5|Briefly described|p410 Fig 1, p411. p423|Paleoproterozoic|Paleoproterozoic|Maximum thickness: 2000m. Underlies the eastern Cariewerloo Basin, extending to the east.|~1650 Ma|||Overlain, likely in fault contact, by the older Labyrinth Formation.|Conglomerate, quartzite and carbonaceous and pyritic siltstones.|
17845|Tarcoola Formation|71799|5|Briefly described|p150 fig 2|Statherian|Statherian|Eastern Gawler Craton.|ca 1650 Ma||||Siltstone, carbonaceous shale and dolomite.|
17845|Tarcoola Formation|71859|5|Briefly described|p5|Statherian|Statherian|Central Gawler Craton.|c. 1655 Ma||||Sandstone, shale, dolomite and dacitic to andesitic volcaniclastic rocks.|
17845|Tarcoola Formation|71862|5|Briefly described|p4, p13, p52|Paleoproterozoic|Paleoproterozoic|Central Gawler Craton.|c. 1655 Ma|||Unconformably overlies the Paxton Granite and the Peter Pan Supersuite.|Sandstone, shale, dolomite and dacitic to andesitic volcanoclastic rocks.|
17845|Tarcoola Formation|72459|6|Mentioned|p51|Palaeoproterozoic|Palaeoproterozoic|Wilgena domain, deposited in localised graben, associated with minor volcanism.|1656 +/- 7 Ma|||||
17845|Tarcoola Formation|73026|6|Mentioned|p10|Statherian|Statherian||c. 1660 Ma|||||
17845|Tarcoola Formation|73027|5|Briefly described|p9,|Mesoproterozoic|Mesoproterozoic|Central Gawler Craton, occurred in a local rift setting.|c. 1660||||Sediments and volcanics.|
17845|Tarcoola Formation|73030|6|Mentioned|p2149|Statherian|Statherian|Gawler Craton.||||||
17845|Tarcoola Formation|73233|6|Mentioned|p27 Fig.1|Paleoproterozoic|Paleoproterozoic|||||||
17845|Tarcoola Formation|73235|6|Mentioned|p53, p59-61, p64|Statherian|Statherian|Gawler Craton. Gawler Range Volcanic, Wilgena and Harris Greenstone regions. Hosts Tarcoola epithermal gold mineralisation in the Tarcoola mineral field of the Kararan (Gawler Range Volcanics) gold mineral system.|1657 Ma|||||
17845|Tarcoola Formation|73302|5|Briefly described|p32||||c.1650 Ma.||||A fault-bound complex of sedimentary rocks and minor intercalated mafic-felsic volcanics.|
17845|Tarcoola Formation|73493|5|Briefly described|p716 Fig.3|||Gawler Craton.|||||Shale, siltstone or schist, conglomerate, mafic volcanics.|
17851|Taringa Formation|22525|4|Described|p37,40||Pleistocene|Superceeded by Ngaltinga Formation||||||
17851|Taringa Formation|22941|6|Mentioned|p290|||||||||
17851|Taringa Formation|23489|6|Mentioned|p43|||||||||
17851|Taringa Formation|39351|6|Mentioned|Map legend|Quaternary|Quaternary|||||||
17851|Taringa Formation|39522|6|Mentioned|p85|||||||||
17851|Taringa Formation|43682|6|Mentioned|p290|||||||||
17851|Taringa Formation|44198|2|Defined|p41|Late Pleistocene|Late Pleistocene|||||||
17851|Taringa Formation|44199|2|Defined|p594, 595, 597|Quaternary|Neogene|late Tertiary - Quaternary. Alluvial||||||
17851|Taringa Formation|65901|4|Described|p176 Tab.1, o178 Fig.1, p179, p185-6|Pleistocene|Pleistocene|Possible mudflow deposit in parts. Probable Taringa Formation material dated at 164+/-17 ka using OSL.||||Overlies Ochre Cove Formation.|Columnar, green-grey clay containing angular clasts and calcium carbonate in upper part.|08-MAR-12
17853|Tarlee Bluestone|40499|6|Mentioned|p149|||||||||
17853|Tarlee Bluestone|61237|6|Mentioned|p36|||Commercial term for historic building stone from the mid-north of South Australia state.||||||
17876|Tartangan beds|34758|6|Mentioned|Table 1|||||||||
17876|Tartangan beds|38383|6|Mentioned|Table 1|||||||||
17876|Tartangan beds|42966|6|Mentioned|p282|||||||||
17933|Telford Gravel|23054|6|Mentioned|p30|||||||||
17933|Telford Gravel|23394|5|Briefly described|Map legend|Cenozoic|Cenozoic|||||||19-NOV-08
17933|Telford Gravel|23719|6|Mentioned|p29|||Geological Province: Gawler Craton.||||||
17933|Telford Gravel|23818|6|Mentioned|p224|||||||||
17933|Telford Gravel|24176|4|Described|p21, p22 Tb. 1|Late Pleistocene|Pleistocene|Polymict gravel, channel sands.  Overlain by Arrowie Formation.  Geological Province: Mount Painter Province.||||||
17933|Telford Gravel|24321|5|Briefly described|Map legend|Pleistocene|Pleistocene|||||||
17933|Telford Gravel|29780|6|Mentioned|p51|||||||||
17933|Telford Gravel|30055|6|Mentioned|p152|||||||||
17933|Telford Gravel|30056|6|Mentioned|p137|||||||||
17933|Telford Gravel|30176|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
17933|Telford Gravel|30177|5|Briefly described|p107|||Pleistocene age.||||||
17933|Telford Gravel|30713|5|Briefly described|p106|||Pleistocene - Recent.||||||
17933|Telford Gravel|30754|6|Mentioned|p22|||Stratigraphic table||||||
17933|Telford Gravel|30802|6|Mentioned|p10|||Pleistocene||||||
17933|Telford Gravel|30804|6|Mentioned|p14|||On Table 1||||||
17933|Telford Gravel|30807|6|Mentioned|p101|||Suggested map symbol||||||
17933|Telford Gravel|30919|6|Mentioned|Map legend|Quaternary|Quaternary|||||||
17933|Telford Gravel|31699|6|Mentioned|p131|||Pleistocene||||||
17933|Telford Gravel|31797|6|Mentioned|Fig. 3|||||||||
17933|Telford Gravel|32441|6|Mentioned|p125|||Geol. plan||||||
17933|Telford Gravel|34011|5|Briefly described|p67|||Pleistocene - Recent||||||
17933|Telford Gravel|34069|6|Mentioned|p1|||Pleist.  See also Fig.2||||||
17933|Telford Gravel|34176|6|Mentioned|p49|||Pleistocene - Recent.||||||
17933|Telford Gravel|34180|6|Mentioned|p220|||||||||
17933|Telford Gravel|34521|5|Briefly described|p156|||||||||
17933|Telford Gravel|35200|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
17933|Telford Gravel|35232|6|Mentioned|p14|||||||||
17933|Telford Gravel|35772|6|Mentioned|p13|||||||||
17933|Telford Gravel|36081|6|Mentioned|p445|||||||||
17933|Telford Gravel|36621|6|Mentioned|Fig.1|||||||||
17933|Telford Gravel|36894|6|Mentioned|Fig.2|||||||||
17933|Telford Gravel|38068|6|Mentioned|p76|||||||||
17933|Telford Gravel|39349|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
17933|Telford Gravel|39352|6|Mentioned|Map legend|Holocene|Pleistocene|Pleistocene to Holocene||||||
17933|Telford Gravel|40926|6|Mentioned|Table 3|||||||||
17933|Telford Gravel|42375|5|Briefly described|Fig.5 P24, Table 1 1|||||||||
17933|Telford Gravel|42720|6|Mentioned|map legend|Pleistocene||||||||
17933|Telford Gravel|42813|6|Mentioned|p25|||||||||
17933|Telford Gravel|42966|5|Briefly described|p214|||||||||
17933|Telford Gravel|43073|6|Mentioned|p17|||||||||
17933|Telford Gravel|43094|5|Briefly described|p40|||||||||
17933|Telford Gravel|44133|5|Briefly described|p241|Pleistocene|Pleistocene|Geological Province: Pirie Basin.||||||
17933|Telford Gravel|44659|5|Briefly described|map legend||Pleistocene|Pleistocene, lithology.||||||
17933|Telford Gravel|44660|14|Not recorded|map legend||Pleistocene|Pleistocene, lithology.||||||
17933|Telford Gravel|45128|6|Mentioned|Fig.42|||Correlation table of sediments containing Dromornithidae in Australia.||||||
17933|Telford Gravel|65925|5|Briefly described|Appendix 2.||||||||Polymict gravel, well rounded, includes boulders. Alluvial fan deposits.|
17933|Telford Gravel|68126|6|Mentioned|p31|Paleozoic|Paleozoic|||||||
17933|Telford Gravel|70333|5|Briefly described|Map legend.|Pleistocene|Pleistocene||||||Polymict gravel, well-rounded, includes boulders. Alluvial fan deposits.|
17933|Telford Gravel|70334|4|Described|p61,64,83|||Of Spencer Gulf area. Thickness: typically 2-3m. Derived from neoproterozoic bedrock of the Adelaide Geosyncline. Occurs in the SE part of CULTANA 10 km south of Mambray Creek, extending eastwards onto ORROROO (Binks, 1966, Binks, 1968). Deposited as alluvial fans flanking the Flinders Ranges (Callen et al., 1995). Consists of an upper and lower member (both unnamed). Overlain by unnamed modern drainage sediments.||||Underlain by Hindmarsh Clay.|Polymict gravel containing well-rounded pebble and boulder clasts of quartz, quartzite, siltstone, shale and dolomite.|14-OCT-19
17933|Telford Gravel|70384|5|Briefly described|Map legend.|Pleistocene|Pleistocene|Alluvial fan deposits.|||||Well-rounded polymict gravel; includes boulders.|
17933|Telford Gravel|73103|5|Briefly described|Map legend.|Pleistocene|Pleistocene||||||Polymict gravel, well-rounded, includes boulders. Alluvial fan deposits.|
17933|Telford Gravel|73110|5|Briefly described|Map legend.|Pleistocene|Pleistocene||||||Polymict gravel, well-rounded, includes boulders. Alluvial fan deposits.|
17959|Tent Hill Formation|22677|5|Briefly described|Fig.2 p735||Neoproterozoic|Age of unit 676+/-204 Ma||||||
17959|Tent Hill Formation|22829|6|Mentioned|Fig2 P17|||||||||
17959|Tent Hill Formation|22921|5|Briefly described|38|||||||||
17959|Tent Hill Formation|23250|5|Briefly described|p1124  Fig.2||Neoproterozoic III|Correlate of Brachina Formation and ABC Range Quartzite (Wilpena Group) and Pertatataka Formation, Gayland Sandstone, Cyclops Member and Waldo Pedlar Member.||||||
17959|Tent Hill Formation|23287|6|Mentioned|Fig.2|||Age: Lower Ediacarian. Of Stuart Shelf.||||||09-MAY-16
17959|Tent Hill Formation|23719|6|Mentioned|p9|||Geological Province: Gawler Craton.||||||07-FEB-18
17959|Tent Hill Formation|23805|5|Briefly described|p5 Fig. 3|Neoproterozoic|Neoproterozoic|Of the Wilpena Group.  Geological Province: Gawler Craton.||||||
17959|Tent Hill Formation|23818|5|Briefly described|p73 Fig.27|Adelaidean|Adelaidean|Of the Wilpena Group. Max. thickness: ~2600 ft.||||||
17959|Tent Hill Formation|23913|4|Described|p110 Fig. 2|Adelaidean|Adelaidean|Geological Province: Sturt Shelf.  Of the Wilpena Group.  Underlying Unit: Nuccaleena Formation.  Overlying Unit: Yarloo Shale.||||||
17959|Tent Hill Formation|24321|5|Briefly described|Map legend|Late Adelaidean|Late Adelaidean|Parent: Wilpena Group||||||
17959|Tent Hill Formation|24476|4|Described|p547 Fig. 4|Vendian|Vendian|Overlies the Nuccaleena Formation. Overlain by the Yarloo Shale. Geological Province: Stuart Shelf.||||||
17959|Tent Hill Formation|29780|6|Mentioned|p42|||||||||
17959|Tent Hill Formation|29838|6|Mentioned|p4|||||||||
17959|Tent Hill Formation|30801|6|Mentioned|p5|||Marinoan. Table P5-6||||||
17959|Tent Hill Formation|30802|6|Mentioned|p12|||||||||
17959|Tent Hill Formation|30807|6|Mentioned|p102|||Suggested map symbol||||||
17959|Tent Hill Formation|31324|5|Briefly described|p158|||||||||
17959|Tent Hill Formation|31395|6|Mentioned|p64|||||||||
17959|Tent Hill Formation|31540|4|Described|p10|||||||||
17959|Tent Hill Formation|31541|6|Mentioned|p547|||||||||
17959|Tent Hill Formation|32507|6|Mentioned|Table 3|||||||||
17959|Tent Hill Formation|33470|6|Mentioned|Table 1|||||||||
17959|Tent Hill Formation|33474|6|Mentioned|Fig.2|||||||||
17959|Tent Hill Formation|34116|5|Briefly described|p17|||Proterozoic. See also PP18-19||||||
17959|Tent Hill Formation|34269|6|Mentioned|Table 1|||||||||
17959|Tent Hill Formation|34319|6|Mentioned|p69|||||||||
17959|Tent Hill Formation|34535|6|Mentioned|p74|||Lower part Wilpena Group||||||
17959|Tent Hill Formation|34536|6|Mentioned|Map legend|Adelaidean|Adelaidean|Marinoan||||||
17959|Tent Hill Formation|34537|6|Mentioned|Fig.7|||||||||
17959|Tent Hill Formation|34610|6|Mentioned|p178|||||||||
17959|Tent Hill Formation|35130|6|Mentioned|p7|||||||||
17959|Tent Hill Formation|35255|6|Mentioned|p10|||||||||
17959|Tent Hill Formation|35548|6|Mentioned|Fig.3|||Andamooka Precious Stones Field.||||||
17959|Tent Hill Formation|35549|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
17959|Tent Hill Formation|36621|6|Mentioned|Fig.1|||||||||
17959|Tent Hill Formation|38022|6|Mentioned|Fig.4|||||||||
17959|Tent Hill Formation|38581|6|Mentioned|p253|||||||||
17959|Tent Hill Formation|38915|6|Mentioned|p343|||Geological Province: New England Fold Belt||||||
17959|Tent Hill Formation|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Marinoan||||||
17959|Tent Hill Formation|39629|6|Mentioned|Fig.1|||||||||
17959|Tent Hill Formation|39724|6|Mentioned|Fig.6|||||||||
17959|Tent Hill Formation|39807|6|Mentioned|p225|||||||||
17959|Tent Hill Formation|39808|6|Mentioned|p223|||||||||
17959|Tent Hill Formation|40257|6|Mentioned|Fig.2|||||||||
17959|Tent Hill Formation|40445|6|Mentioned|p53|||||||||
17959|Tent Hill Formation|40448|5|Briefly described|p38|||||||||
17959|Tent Hill Formation|40811|6|Mentioned|p319|||||||||
17959|Tent Hill Formation|41005|6|Mentioned|p217|||||||||
17959|Tent Hill Formation|41429|3|Fully described|p223|||||||||
17959|Tent Hill Formation|41493|6|Mentioned|Table 1|||||||||
17959|Tent Hill Formation|41507|6|Mentioned|p17|||||||||
17959|Tent Hill Formation|41667|6|Mentioned|Fig.3|||||||||
17959|Tent Hill Formation|41703|6|Mentioned|p243|||||||||
17959|Tent Hill Formation|42088|5|Briefly described|p544|||||||||
17959|Tent Hill Formation|42222|6|Mentioned|p19|||||||||
17959|Tent Hill Formation|42247|5|Briefly described|Fig.3 P7|||||||||
17959|Tent Hill Formation|42346|5|Briefly described|p77, Fig.2 p79|||||||||
17959|Tent Hill Formation|42465|5|Briefly described|Map legend|||||||||
17959|Tent Hill Formation|42469|5|Briefly described|p24, p23|||||||||
17959|Tent Hill Formation|42546|5|Briefly described|Map legend|Adelaidean (Marinoan)||||||||
17959|Tent Hill Formation|42600|6|Mentioned|p9|||||||||
17959|Tent Hill Formation|42721|5|Briefly described|map legend|Marinoan||||||||
17959|Tent Hill Formation|42723|5|Briefly described|map legend|Marinoan||||||||
17959|Tent Hill Formation|42736|5|Briefly described|map legend|Neoproterozoic||||||||
17959|Tent Hill Formation|43048|4|Described|Table 1.|||||||||
17959|Tent Hill Formation|43052|5|Briefly described|p192,table 6.1|||of Wilpena Group||||||
17959|Tent Hill Formation|43085|5|Briefly described|Fig.5|||||||||
17959|Tent Hill Formation|43094|4|Described|p34,Table 5.|||||||||
17959|Tent Hill Formation|43622|6|Mentioned|p38|Neoproterozoic||||||||
17959|Tent Hill Formation|44133|5|Briefly described|p24|||Underlies: Andamooka Limestone.||||||
17959|Tent Hill Formation|44538|4|Described|map legend|||(H53-16). Geol.Atlas Series. Includes the topmost member, Arcoona Quartzite Member. Marinoan.||||||
17959|Tent Hill Formation|44660|14|Not recorded|map legend|||Marinoan.||||||
17959|Tent Hill Formation|44689|14|Not recorded|map legend||Adelaidean|Andamooka. (H53-12). Contains Arcoona Quartzite & Woomera Shale Members. Top of Adelaidean.||||||
17959|Tent Hill Formation|44690|4|Described|map legend|||Geol. Atlas Series. (I/54-5). Includes Simmens Member. Marinoan.||||||
17959|Tent Hill Formation|44934|5|Briefly described|Map Legend||Adelaidean|||||||
17959|Tent Hill Formation|60955|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Includes Arcoona Quartzite Member, Corraberra Sandstone Member, Woomera Shale Member. Of the Wilpena Group.||||||13-APR-05
17959|Tent Hill Formation|61732|6|Mentioned|p26, p133|||Superseded by ABC Range Quartzite. Geological Province: Stuart Shelf.||||||07-FEB-11
17959|Tent Hill Formation|65483|6|Mentioned|p19, Fig 2|Neoproterozoic|Neoproterozoic|Of the Wilpena Group. Overlies Umberatana Group.||||||28-JAN-11
17959|Tent Hill Formation|67870|6|Mentioned|p18|||Mapped in the PORT AUGUSTA 1:250 000 geological map.|||Corraberra Sandstone Member.|||
17959|Tent Hill Formation|69666|6|Mentioned|p25|||||||||
17959|Tent Hill Formation|70082|5|Briefly described|p2|Ediacaran|Ediacaran|Stuart Shelf. Contains red beds.||||||
17959|Tent Hill Formation|70334|4|Described|p2-3,20,38,52,55-59,66,68,77,82,88,92|Tonian|Tonian|Geological province: Gawler Craton. Of Stuart Shelf. Coarsening-upwards shelfal sequence representing rapid marine transgression during interglacial period after Sturtian glaciation. Exposed on the Stuart Shelf as a prominent tableland. Intruded by Jurassic Kimberlitic magmatism associated with Australia-Gondwana magmatism.||Unit of Sandison Subgroup.|Includes Tregolana Shale Member, Corraberra Sandstone Member and Simmens Quartzite Member.|overlain by Yarloo Shale. Equivalent to Brachina Formation and ABC Range Quartzite.|Coarsening-upwards sequence of shale and sandstone.|
17959|Tent Hill Formation|70406|4|Described|p121-124, p119-121, 126, 127, 117|Neoproterozoic|Neoproterozoic|~200m thick at South Tent Hill.||Of Sandison Subgroup.|Includes from base upwards: Tregolana Shale Member, Lincoln Gap Siltstone Member, Corraberra Sandstone Member|Gradationally overlain by Simmens Quartzite. Correlated with Brachina Formation.||29-APR-16
17959|Tent Hill Formation|70659|6|Mentioned|p10|Neoproterozoic|Neoproterozoic|||||||
17959|Tent Hill Formation|70816|6|Mentioned|p3|Neoproterozoic|Neoproterozoic|Gawler Ranges region.||||||
17959|Tent Hill Formation|70948|6|Mentioned|p974|Neoproterozoic|Neoproterozoic|Geological province: Gawler Craton.||||||
17959|Tent Hill Formation|71037|5|Briefly described|p21 Fig.1, p22-23 Fig.2, p27 Fig.6|Neoproterozoic|Neoproterozoic|Age shown as Marinoan.||Wilpena Group|Includes Simmens Quartzite Member, Corraberra Sandstone Member, Lincoln Gap Siltstone Member, Tregolana Shale Member.|Shown as younger than Upalinna and Yerelina Subgroups.|White, red and purple shale, sandstone and quartzite; laminated; slumped.|
17959|Tent Hill Formation|71129|4|Described|p1,15,111-112,126,128-129,131|Ediacaran|Ediacaran|Of Stuart Shelf. Type section: southern part of South Tent Hill (Thomson, 1965, Dalgarno et al., 1968, Dyson, 1996). Deposited during rapid marine transgression in a shallow marine, storm-dominated shelf environment. Coarsening-upwards shale and sandstone sequence, dominantly representing the Simmens Plateau. Crops out along the eastern margin of, and around the NE corner of SIX MILE HILL. Intruded by kimberlites during the Jurassic, associated with Gondwanan breakup. See also p134,138, p145, 150,164-165,184,208-209,225,227.||Unit of Wilpena Group.|Includes Simmens Quartzite Member, Corroberra Sandstone member, Lincoln Gap Siltsone Member and Tregolana Shale.|Overlain by Yarloo Shale and Andamooka Limestone. Broadly equivalent to ABC Range Quartzite and Brachina Formation. Underlain by Umberatana Group.|White, red and purple shale, sandstone and quartzite; laminated; slumped. In places the shales and siltstones are completely weathered to kaolinitic saprolite.|13-NOV-19
17959|Tent Hill Formation|71130|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|||Wilpena Group.|Tregolana Shale Member.||White, red and purple shale, sandstone and quartzite; laminated, slumped.|
17959|Tent Hill Formation|71131|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|||Wilpena Group.|Tregolana Shale, Lincoln Gap Siltstone, Corraberra Sandstone, Simmens Quartzite, Members.||White, red and purple shale, sandstone and quartzite; laminated, slumped.|
17959|Tent Hill Formation|71236|5|Briefly described|p3 fig 2, p28|Marinoan|Marinoan|Cultana Inlier, Gawler Craton.||||||17-MAR-23
17959|Tent Hill Formation|71242|5|Briefly described|p9, 10,11|||||||||07-FEB-18
17959|Tent Hill Formation|71559|6|Mentioned|p15 Fig 1|Neoproterozoic|Neoproterozoic|Geological province: Gawler Craton.||||||
17959|Tent Hill Formation|71859|6|Mentioned|p6|Neoproterozoic|Neoproterozoic|Gawler Craton. Outcrops on the Eyre Peninsula.||||||
17959|Tent Hill Formation|71895|6|Mentioned|App4. p4,|||Punt Hill Region.||||||28-OCT-22
17959|Tent Hill Formation|72247|6|Mentioned|p41-42|Neoproterozoic|Neoproterozoic|Of Adelaide Geosyncline. Nomenclature originally of Thomson and Johnson 1968.|||Includes Whyalla Sandstone Member.|||
17959|Tent Hill Formation|72463|6|Mentioned|p2|Neoproterozoic|Neoproterozoic|||||||
17959|Tent Hill Formation|73130|6|Mentioned|[poster] Fig.1|Neoproterozoic|Neoproterozoic|||||||28-OCT-22
17959|Tent Hill Formation|73227|5|Briefly described|p25|Ediacaran|Ediacaran|Torrens Hinge Zone and[?] Woomera area. Named after the flat-topped buttes this unit forms on the southern Stuart Shelf, including Mount Gunson and Arcoona Plateau.||Wilpena Group|Tregolana Shale Member, Corraberra Sandstone Member, Simmens Quartzite Member|||
17959|Tent Hill Formation|73234|4|Described|p6, p12, p20|early Ediacaran|early Ediacaran|Deposited in marine environments, initially under low-energy conditions in greater water depths but gradually changing with time to higher energy conditions in shallow waters. Affected by paleolandslides.|After 635 Ma|Wilpena Group|Tregolana Shale Member, Lincoln Gap Siltstone Member, Corraberra Sandstone Member, Simmens Quartzite Member|Underlain by Nuccaleena Formation.|Shaly to sandy coarsening-upwards succession.|
17992|Terrapinna Granite|22631|6|Mentioned|p176|Calymmian|Calymmian|||||||
17992|Terrapinna Granite|23385|6|Mentioned|Table 2|||||||||
17992|Terrapinna Granite|23394|5|Briefly described|Map legend|Proterozoic|Proterozoic|||||||
17992|Terrapinna Granite|23411|6|Mentioned|Map Legend|||||||||
17992|Terrapinna Granite|23478|5|Briefly described|p27|Mesoproterozoic|Mesoproterozoic|||||||
17992|Terrapinna Granite|23775|6|Mentioned|p728|||||||||22-SEP-09
17992|Terrapinna Granite|23804|6|Mentioned|p17|||||||||
17992|Terrapinna Granite|23818|6|Mentioned|p37|||||||||
17992|Terrapinna Granite|24176|4|Described|p9, p26 Tb. 1|Proterozoic|Proterozoic|Of "Older Granite Suite".  Rapakivi-like granite, minor adamellite, augen gneiss.  Age is Carpentarian.  Geological Province: Mount Painter Province.||||||
17992|Terrapinna Granite|30176|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
17992|Terrapinna Granite|30177|2|Defined|p126|Precambrian|Precambrian|See also p44. Type area: Hamilton Creek, 0.3 miles south of Terrapinna Waterhole [probably Terrapinna Springs], lat. 29degrees 54'55" S long. 139degrees 40'08"E. [location mistakenly given as 25 degress 54'55" S]||||||24-NOV-22
17992|Terrapinna Granite|30178|6|Mentioned|p20|||||||||
17992|Terrapinna Granite|30807|6|Mentioned|p103|||Suggested map symbol||||||
17992|Terrapinna Granite|30920|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
17992|Terrapinna Granite|32364|6|Mentioned|p17|||||||||
17992|Terrapinna Granite|34537|6|Mentioned|p37|||||||||
17992|Terrapinna Granite|35255|6|Mentioned|Fig.24|||||||||
17992|Terrapinna Granite|35602|6|Mentioned|p152|||||||||
17992|Terrapinna Granite|41405|5|Briefly described|p128|||||||||
17992|Terrapinna Granite|42105|6|Mentioned|Fig.1 P87|||||||||
17992|Terrapinna Granite|42602|5|Briefly described|p20,p19|||||||||
17992|Terrapinna Granite|42624|4|Described|p23|||||||||
17992|Terrapinna Granite|42885|6|Mentioned|p27|||||||||
17992|Terrapinna Granite|43052|5|Briefly described|p153|||||||||
17992|Terrapinna 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: 1556-1557 +/- 6Ma (U-Pb).||||||
17992|Terrapinna Granite|62962|5|Briefly described|p2284 Fig. 2|Mesoproterozoic|Mesoproterozoic|Age: 1556+/-4Ma (Thornton, 1980). Geological Province: Mount Painter Province.||||||07-FEB-11
17992|Terrapinna Granite|65925|5|Briefly described|Appendix 2.||||||||Granite, grey, ovoid K feldspar megacrysts.|
17992|Terrapinna Granite|66302|6|Mentioned|p50, p78|Calymmian|Calymmian|Moolawatana Domain, Curnamona Province. Ages are derived from Sheard et al. (1992) and Fraser and Neumann (2010) respectively.|1557 +/- 6 Ma to 1560 +/- 3 Ma|Moolawatana Suite||||
17992|Terrapinna Granite|68068|5|Briefly described|Map legend|||Curnamona Province. Local intimate apophyses with the older Wattleowie Granite are mapped separately.|1557 +/- 6 Ma; 1556 +/- 4 Ma (U-Pb zircon).|Unit in Moolawatana Suite.|||Massive to gneissic, coarse-grained grey porphyritic rapakivi-like granite to adamellite (pink weathering); minor comagmatic varieties including melanocratic, medium-grained and a sparsely-porphyritic to xenocrystic form.|
17992|Terrapinna Granite|68205|5|Briefly described|p84-86,89-90,92,94-95,99,101-102|Calymmian|Calymmian|Geological province: Curnamona Province. Less evolved samples contain titanite, more evolved samples are peraluminous and contains garnet, chlorite and muscovite, and occasionally Fe Ti-oxides and rutile. Geochemical analysis provided from p88-92. Nd isotope analysis on p92-94. U-Pb zircon geochronology on p94-99. Ages reported: 1560+\-3 Ma (Fraser and Neumann 2010); 1556+\-4 Ma and 1557+\-6 Ma (Stewart and Foden 2001); and 1572+\-15 Ma (Wulser 2009). Exposed in Mount Painter and Mount Babbage Inlier.|1545-1555 Ma|Unit of Moolawatana Suite.|||Pink-orange, equigranular and partly porphyritic granite.|02-JUL-19
17992|Terrapinna Granite|68713|6|Mentioned|p19||||||||Coarse-grained porphyritic texture. Grey with bluish and grey phenocrysts when fresh.|
17992|Terrapinna Granite|69019|4|Described|p16, p26-29, p64-65, p92 Fig.22.|Calymmian|Calymmian|Curnamona Province. Coats and Blissett (1971). Includes enclaves of Wattleowie Granite. Resembles rapakivi texture. Geochemistry is detailed, and resembles Wattleowie Granite. Middle level intrusion. Has potential for dimension stone extraction.|1557 +/- 6 Ma (U-Pb zircon: Callen et al 1990).|Unit in Moolawatana Suite.||Intrudes Radium Creek Group. Intruded by Mudnawatana Tonalite dykes. Is overlain unconformably by Parabarana Sandstone.|Very coarse-grained, K-feldspar megacrystic massive biotite granite, biotite monzogranite; rare tonalite.|
17992|Terrapinna Granite|69023|3|Fully described|p17, p21-28, p34, p37, p42-45, p47-49|Mesoproterozoic|Mesoproterozoic|See also p52-54, p64, p77, p86-88, p98, p101, p143-146, p154, p162, p189, p202. Coats and Blissett (1971). Part of the crystalline basement in Mount Babbage and Mount Painter Inliers. Middle level emplacement. Geochemistry detailed. Trace element abundances are similar to Mount Neill Granite. Includes xenoliths of Yerila and (the possibly comagmatic) Wattleowie Granites. One variant strongly resembles Prospect Hill Granite. Locally hydrothermally altered.  U-Pb zircon age by Thornton (1980), modified by Cooper et al. (1982). Other similar ages given. Rapakivi variant has potential for dimension stone.|1556 +/- 4 Ma.|Unit in Moolawatana Suite.||Intrudes Brindana Schist, Yerila and Wattleowie Granites. Is intruded by Con Bore and Golden Pole Granites, and Mudnawatana Tonalite.|A distinctive coarse-grained, ovoid K-feldspar and bluish quartz megacrystic, massive crystalline rock; grey, weathering to pinkish, yellow or brown.|
17992|Terrapinna Granite|69562|5|Briefly described|p670 Tb.5||||1560 +/- 3 Ma (Fraser and Neumann, 2010).||||Coarse-grained granite.|
17992|Terrapinna Granite|69650|5|Briefly described|p62, p68|Calymmian|Calymmian|Suggested to come from the same magma source as Coulthard Suite and Pepegoona Porphyry.|~1560 Ma.|Unit in Moolawatana Suite.||||
17992|Terrapinna Granite|70384|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Contains metasediments and granite enclaves. Locally has associated apophyses. Mineralogy: ovoid microcline and ovoid quartz phenocrysts in a mosaic of K-feldspar, quartz, biotite, muscovite, albite. Accessory tourmaline, opaques, apatite, zircon. Both U-Pb zircon ICPMS age determinations. Four intermediate ages are also given.|1572 +/- 15 Ma to 1545 +/- 6 Ma U/Pb ICPMS.|||Intrudes Wattleowie Granite.|Massive to gneissic, coarse-grained grey porphyritic rapakivi-like granite to quartz monzonite (pink weathering). Minor co-magmatic melanocratic, medium-grained varieties and a sparsely megacrystic member (mapped separately).|17-JAN-19
17992|Terrapinna Granite|71531|14|Not recorded|p8, 9, 10||Carpentarian|||||||
17992|Terrapinna Granite|72456|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Marree 1:250k map sheet.|||||Granite, grey, ovoid, K-feldspar megacrysts.|
17992|Terrapinna Granite|72459|4|Described|p63-66, p73, p82-89, p94-99|Mesoproterozoic|Mesoproterozoic|Together with the Wattleowie granite, White Well Granite, Golden Pole granite and the Petermorra Volcanics forms sub""group"" 2b of this report. In outcrop this unit often exhibits complex, intermingled association with the Wattleowie granite. Displays decreasing LREE, Th, U and Nb with increasing silica. An additional date is 1557 +/- 6 Ma (Sheard et al, 1992).|1556 +/- 4 Ma (Thornton, 1980);|Moolawatana Suite||Intrudes the Yerila Granite.|White to pale grey, megacrystic biotite granite.|
17992|Terrapinna Granite|73061|4|Described|p1067, p1069, p1071-1072, p1076-1077|Calymmian|Calymmian|Mount Painter Province, Mount Babbage Inlier and northern Mount Painter Inlier. High heat producing granite. Gradational contact with Wattleowie Granite suggests it to be comagmatic. SHRIMP U-Pb zircon crystallisation ages of 1557 +/- 6 Ma (Sheard et al., 1992), 1560 +/- 3 Ma (Fraser and Neumann, 2010). Mean eHf value of +1.0 +/- 1.3. 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, Fig.2, p1074.|1565 +/- 18 Ma U-Pb LA-ICPMS, 1557 +/- 6 Ma|||Intruded by the Wattleowie Granite.|Pale grey and medium- to coarse-grained granite containing megacrystic K-feldspar and plagioclase phenocrysts. Includes coarse-grained rapakivi-like granite.|
18066|Thompson Creek Formation|30176|6|Mentioned|Map legend|Recent|Recent|||||||
18066|Thompson Creek Formation|31895|4|Described|Table 1|||Holocene||||||
18066|Thompson Creek Formation|40439|6|Mentioned|p383|||||||||
18082|Thorndale Composite Gneiss|6823|6|Mentioned|p205|Palaeoproterozoic|Palaeoproterozoic|||||Underlies the Thackaringa Group.||26-MAR-22
18082|Thorndale Composite Gneiss|22553|5|Briefly described|fig2p77,p78|Proterozoic|Proterozoic|||||||
18082|Thorndale Composite Gneiss|22575|6|Mentioned|p179 Fig.2|||In the Broken Hill Block.||||||11-JUN-08
18082|Thorndale Composite Gneiss|22588|6|Mentioned|p85|||||||||
18082|Thorndale Composite Gneiss|22631|6|Mentioned|table1, p173|Statherian|Statherian|||||||
18082|Thorndale Composite Gneiss|22771|6|Mentioned|Table12.2p45|||||||||
18082|Thorndale Composite Gneiss|22857|4|Described|p45 Tb. 12.2, p392 App1 Tb.A1.1|Paleoproterozoic|Paleoproterozoic|Formerly the Thorndale Gneiss of Mawson (1912). Of the Willyama Supergroup. Max. thickness: 2km; in type section: 1400m. Geological Province: Willyama Fold Belt.||||||07-NOV-08
18082|Thorndale Composite Gneiss|22884|5|Briefly described|p41|||Overlain by units of Thackeringa Group. Geological province: Broken Hill Domain.||||||26-MAR-09
18082|Thorndale Composite Gneiss|22959|6|Mentioned|p95||Paleoproterozoic|||||||07-NOV-08
18082|Thorndale Composite Gneiss|22962|6|Mentioned|p74||Statherian|||||||
18082|Thorndale Composite Gneiss|22963|5|Briefly described|p69||Paleoproterozoic|Possible correlation with Gandry Dam Gneiss (Mt Isa Maronan Supergroup) and lower sequence of the Georgetown (Qld) Etheridge Group.||||||07-NOV-08
18082|Thorndale Composite Gneiss|22965|6|Mentioned|p13, Fig1||Statherian|||||||
18082|Thorndale Composite Gneiss|22966|6|Mentioned|Fig1||Proterozoic|Rift stage of development.||||||
18082|Thorndale Composite Gneiss|22967|5|Briefly described|p25,6,39,41||Statherian|||||||
18082|Thorndale Composite Gneiss|23025|6|Mentioned|Fig1p75|||||||||
18082|Thorndale Composite Gneiss|23160|6|Mentioned|fig1|||||||||
18082|Thorndale Composite Gneiss|23248|5|Briefly described|Fig2p169|||||||||
18082|Thorndale Composite Gneiss|23347|6|Mentioned|p52|||Geological province: Broken Hill Domain. Equivalent to parts of Wiperaminga Subgroup.||||||24-MAR-09
18082|Thorndale Composite Gneiss|24307|5|Briefly described|p967 Fig. 2|Proterozoic|Proterozoic|||||||
18082|Thorndale Composite Gneiss|38969|4|Described|p204|||||||||
18082|Thorndale Composite Gneiss|39662|2|Defined|p412|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
18082|Thorndale Composite Gneiss|39828|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
18082|Thorndale Composite Gneiss|39849|6|Mentioned|p86|||||||||
18082|Thorndale Composite Gneiss|39883|6|Mentioned|p380|||||||||
18082|Thorndale Composite Gneiss|40290|6|Mentioned|Fig.2|||||||||
18082|Thorndale Composite Gneiss|40595|6|Mentioned|p86|||||||||
18082|Thorndale Composite Gneiss|40822|6|Mentioned|Fig.2|||||||||
18082|Thorndale Composite Gneiss|41093|4|Described|p251|||||||||
18082|Thorndale Composite Gneiss|41145|6|Mentioned|Fig.4|||||||||
18082|Thorndale Composite Gneiss|41630|6|Mentioned|p27|||||||||
18082|Thorndale Composite Gneiss|41633|6|Mentioned|p141|||||||||
18082|Thorndale Composite Gneiss|42261|6|Mentioned|Fig 1 P530|||||||||
18082|Thorndale Composite Gneiss|42507|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
18082|Thorndale Composite Gneiss|42527|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
18082|Thorndale Composite Gneiss|42528|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
18082|Thorndale Composite Gneiss|42537|6|Mentioned|Fig.2 P5|||||||||
18082|Thorndale Composite Gneiss|42595|6|Mentioned|Fig. 2 P5|||||||||
18082|Thorndale Composite Gneiss|42720|5|Briefly described|map legend|Paleoproterozoic||South Australia.||||||07-NOV-08
18082|Thorndale Composite Gneiss|42813|6|Mentioned|p9|||||||||
18082|Thorndale Composite Gneiss|42897|5|Briefly described|Fig.3, P321|||||||||
18082|Thorndale Composite Gneiss|42942|6|Mentioned|p17|||Of Willyama Supergroup.||||||11-JUN-08
18082|Thorndale Composite Gneiss|43052|6|Mentioned|Fig.4.22|||||||||
18082|Thorndale Composite Gneiss|43086|6|Mentioned|Fig.3|||||||||
18082|Thorndale Composite Gneiss|43263|6|Mentioned|Map Legend||Paleoproterozoic|||||||07-NOV-08
18082|Thorndale Composite Gneiss|43268|5|Briefly described|Map Legend||Paleoproterozoic|Of Willyama Supergroup.||||||07-NOV-08
18082|Thorndale Composite Gneiss|43270|5|Briefly described|Map Legend||Paleoproterozoic|Of the Willyama Supergroup.||||||07-NOV-08
18082|Thorndale Composite Gneiss|43271|5|Briefly described|Map Legend||Paleoproterozoic|Of Willyama Supergroup.||||||07-NOV-08
18082|Thorndale Composite Gneiss|43272|5|Briefly described|Map Legend||Paleoproterozoic|Of the Willyama Supergroup.||||||07-NOV-08
18082|Thorndale Composite Gneiss|43274|5|Briefly described|Map Legend||Paleoproterozoic|Of Willyama Supergroup.||||||07-NOV-08
18082|Thorndale Composite Gneiss|43572|6|Mentioned|Fig.3.2 p6|||||||||
18082|Thorndale Composite Gneiss|43583|5|Briefly described|Table 1, p2139|||||||||
18082|Thorndale Composite Gneiss|46598|5|Briefly described|p303|||||||||
18082|Thorndale Composite Gneiss|50045|5|Briefly described|p116 Fig. 3, p114 Fig. 1|||Geological Province: Broken Hill Block. Of the Willyama Supergroup. Overlain by Thackaringa Group. Underlain by Clevedale Migmatite.||||||31-MAY-07
18082|Thorndale Composite Gneiss|50619|5|Briefly described|p174 Fig. 1|Paleoproterozoic|Paleoproterozoic|Of the Willyama Supergroup. Metasedimentary pelitic to psammitic gneiss. Geological Province: Broken Hill Block.||||||07-SEP-15
18082|Thorndale Composite Gneiss|60485|5|Briefly described|p28 Fig. 2|||Of the Thackaringa Group? Geological Province: Broken Hill Domain.||||||
18082|Thorndale Composite Gneiss|61606|5|Briefly described|p4 Fig.2|||Of the Willyama Supergroup.||||||
18082|Thorndale Composite Gneiss|61735|5|Briefly described|p635 Fig. 1, p653, 639|Paleoproterozoic|Paleoproterozoic|Overlies Clevedale Migmatite. See also p636 Fig. 2. Max depositional age 1830-1850 Ma. Max metamorphic age 1617+/-3 Ma U/Pb SHRIMP.||||||04-JUN-15
18082|Thorndale Composite Gneiss|61736|5|Briefly described|p666 Fig. 3|Paleoproterozoic|Paleoproterozoic|Age: </-1830-1850Ma. Geological province: Olary Domain.||||||24-FEB-10
18082|Thorndale Composite Gneiss|62473|5|Briefly described|p74|Paleoproterozoic|Paleoproterozoic|Apparent ages: 1640 to 1610Ma and older (SHRIMP zircon).||||||17-JUN-09
18082|Thorndale Composite Gneiss|62535|5|Briefly described|p666-667, p672|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain. Hosts various types of oxide-, sulfide-, and silicate-facies iron formation with minor strata-bound Cu, Co and/or Au deposits.|1850-c.1830 Ma.|||||
18082|Thorndale Composite Gneiss|62536|5|Briefly described|p635-636, 639-641, 653-654|||13 km E of Broken Hill. Zircon dating discussed. An alternative dating based on 5 analyses gives an MDA of 1850-1830 Ma.|1617 +/- 3 Ma (metamorphosed; MDA).|||Overlies Clevedale Migmatite. Is overlain by the Thackaringa Group.|Includes metapsammites and pervasive migmatitic segregations. Granulite facies metamorphism.|
18082|Thorndale Composite Gneiss|62592|6|Mentioned|p16 Fig.2.2. |||Broken Hill Domain, Curnamona Province.||Unit in Thackaringa Group.||||
18082|Thorndale Composite Gneiss|62993|6|Mentioned|p37|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain.||Willyama Supergroup|Includes Clevedale Migmatite Member|||15-DEC-21
18082|Thorndale Composite Gneiss|63102|5|Briefly described|p13-15|Statherian|Statherian|Geological province: Broken Hill Domain, Curnamona Province.||Unit of Thackaringa Group.||||
18082|Thorndale Composite Gneiss|63186|5|Briefly described|p71 Fig. 5|Paleoproterozoic|Paleoproterozoic|Age: 1715 Ma. Geological Province: Curnamona Province.||||||07-NOV-08
18082|Thorndale Composite Gneiss|63489|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Metasedimentary composite gneiss.||||||07-NOV-08
18082|Thorndale Composite Gneiss|63519|5|Briefly described|p10 Fig. 3|Paleoproterozoic|Paleoproterozoic|Geological Province: Broken Hill Block-Euriowie Block.||||||07-NOV-08
18082|Thorndale Composite Gneiss|63866|5|Briefly described|p36||||c. 1710 Ma (Max. deposition)|Willyama Supergroup||||
18082|Thorndale Composite Gneiss|64097|5|Briefly described|p303, p325|Paleoproterozoic|Paleoproterozoic|Conformably overlain by Thackaringa Group. Geological province: Broken Hill Domain/Curnamona province. Partially melted metasediments with or without albitic alteration.||||||07-FEB-11
18082|Thorndale Composite Gneiss|64316|5|Briefly described|p533 Fig. 1|Paleoproterozoic|Paleoproterozoic|Geological Province: Broken Hill Block.||||||07-FEB-11
18082|Thorndale Composite Gneiss|64742|6|Mentioned|p321 Fig.3, p323.|||A sample of this unit used for Sm-Nd analysis is listed under Thackaringa Group in Table 1, despite a clear separation of these units in Fig.3.||Unit in Willyama Supergroup.||||29-MAR-12
18082|Thorndale Composite Gneiss|64743|6|Mentioned|p339 Fig.1. |Paleoproterozoic|Paleoproterozoic|||||||
18082|Thorndale Composite Gneiss|64744|5|Briefly described|p353 Fig.4, p354.|Statherian|Statherian|Broken Hill Domain. High-grade metasedimentary rocks.||Unit in Willyama Supergroup.||Overlies Clevedale Migmatite. Is overlain by Thackaringa Group.||
18082|Thorndale Composite Gneiss|64944|5|Briefly described|p28 Fig. 1|Paleoproterozoic|Paleoproterozoic|Geological province: Broken Hill Domain.||||||07-FEB-11
18082|Thorndale Composite Gneiss|66302|5|Briefly described|p36 Fig.9, p39, p40|Statherian|Statherian|Broken Hill Domain, Curnamona Province.|ca. 1710 (U-Pb zircon)|Thackaringa Group||Overlies the Clevedale Migmatite. Overlain by the Lady Brassey Formation.||
18082|Thorndale Composite Gneiss|66857|6|Mentioned|p972 Fig.2.|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain.||Unit in Willyama Supergroup.||Overlies Clevedale Migmatite. Is overlain by Thackaringa Group.||
18082|Thorndale Composite Gneiss|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Broken Hill Domain.|~1850-1830 Ma (max depositional age).|Thackaringa Group.|Clevedale Migmatite Member.|||
18082|Thorndale Composite Gneiss|68067|6|Mentioned|Map legend.|||||||||27-AUG-13
18082|Thorndale Composite Gneiss|68126|5|Briefly described|p6, p29|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain, Curnamona Province.||Willyama Supergroup.||||
18082|Thorndale Composite Gneiss|69999|6|Mentioned|p3|Paleoproterozoic|Paleoproterozoic|Curnamona Province. Basal, early-rift fluviatile to shallow marine sedimentation.||||||
18082|Thorndale Composite Gneiss|70000|5|Briefly described|p31, p33-35|||Among the oldest outcropping units in the Broken Hill Domain.|||Includes Clevedale Migmatite.||Metasedimentary gneiss and migmatite +/- albitic horizons hosting ubiquitous sills and dykes of basic gneiss.|
18082|Thorndale Composite Gneiss|70014|5|Briefly described|Map legend|||Segregations commonly disrupt bedding. Bedding in the composite gneiss/metasediments is generally disrupted, lenticular and/or discontinuous, and highly variable in thickness. Rare graded bedding, crossbedding, and scour-and-fill structures are present in places. Other rocks present include psammitic, psammopelitic and pelitic metasediments, basic gneiss, minor plagioclase-quartz rock and K-feldspar-rich leucocratic rock, and rare quartz-magnetite and quartz-iron oxide/sulfide rocks.||Unit in Willyama Supergroup.||Overlies Clevedale Migmatite. Is overlain by Alma Gneiss (Thackaringa Group).|Mainly metasedimentary quartz-feldspar-biotite-sillimanite +/- garnet +/- cordierite composite gneiss consisting of interlayered psammite and psammopelite, generally with minor pelite; abundant pegmatitic to granitic quartzo-feldspathic segregations.|
18082|Thorndale Composite Gneiss|70015|5|Briefly described|Map legend|Statherian|Statherian|Mineral deposits (if any) are shown.||Unit in Willyama Supergroup.|Includes Clevedale Migmatite.||Metasedimentary (psammite/psammopelite) quartz-feldspar-biotite-sillimanite(-garnet)(-cordierite) composite gneiss, abundant pegmatitic/granitic segregations.|
18082|Thorndale Composite Gneiss|70657|4|Described|p10 Fig.4, p13 Fig.6, p15|Statherian|Statherian|Curnamona Province; Mulyungarie, Broken Hill Domains. Shown as Thackaringa Group + Thorndale Composite Gneiss + Clevedale Migmatite in Fig.4.|~1705-1700 Ma|Thackaringa Group|Includes Clevedale Migmatite.|Overlies Redan Gneiss. Underlies Lady Brassey Formation, and Alma Gneiss of Silver City Suite.||
18082|Thorndale Composite Gneiss|70658|6|Mentioned|p15-16|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain, Curnamona Province.||||||
18082|Thorndale Composite Gneiss|71968|6|Mentioned|p4|||Geological province: Curnamona province.||||||
18082|Thorndale Composite Gneiss|72454|6|Mentioned|p2 Fig.2, p8 Fig.6|Mesoproterozoic|Mesoproterozoic|Part of the Broken Hill Domain. Shown only on p2 Fig.2 and p8 Fig.6.||Willyama Supergroup|||Includes gneiss.|
18082|Thorndale Composite Gneiss|72461|6|Mentioned|p16 fig 9|||||||||
18082|Thorndale Composite Gneiss|73243|6|Mentioned|p52 Fig.1, p53 Fig.2, p59|||Broken Hill block-Euriowie block. Some amphibolite bodies appear to transgress bedding, interpreted as dykes emplaced during or immediately after deposition of the Broken Hill Group. Amphibolite is used in text to refer to all highly metamorphosed pre-1600 Ma mafic rocks including hornblende granulites and pyroxene granulites.||Willyama Supergroup|||Contains amphibolite dykes.|
18082|Thorndale Composite Gneiss|73308|6|Mentioned|p607 Fig.1|||||Willyama Supergroup.||||
18082|Thorndale Composite Gneiss|73482|5|Briefly described|p422 Fig.3, p423|||||Willyama Supergroup|Clevedale Migmatite|||
18082|Thorndale Composite Gneiss|73512|6|Mentioned|p2, p7|||||Willyama Supergroup||||
18082|Thorndale Composite Gneiss|73524|6|Mentioned|p5 Fig.3|||||Thackaringa Group||||
18082|Thorndale Composite Gneiss|73575|5|Briefly described|p828 Fig.2, p829 Fig.3|||||Willyama Supergroup|Clevedale Migmatite|Underlies Thackaringa Group, Lady Brassey Formation||
18197|Tindelpina Shale Member|9862|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Of the Tapley Hill Formation. Finely laminated carbonaceous pyritic shale; minor dolomite.||||||
18197|Tindelpina Shale Member|22510|5|Briefly described|table1p37|||Of the Tapley Hill Formation.  Age: Sturtian||||||13-OCT-04
18197|Tindelpina Shale Member|22631|6|Mentioned|p178|||Age: Sturtian||||||
18197|Tindelpina Shale Member|22772|5|Briefly described|Table13.1|Neoproterozoic III|Neoproterozoic III|||||||
18197|Tindelpina Shale Member|22857|5|Briefly described|Tb. 13.1 (insert p70-71)|Sturtian|Sturtian|Of the Farina Subgroup (Umberatana Formation).||||||
18197|Tindelpina Shale Member|23394|5|Briefly described|Map legend|Proterozoic|Proterozoic|||||||
18197|Tindelpina Shale Member|23411|6|Mentioned|Map Legend|||||||||
18197|Tindelpina Shale Member|23818|5|Briefly described|p64 Fig.22, p66|Neoproterozoic|Neoproterozoic|Basal unit of the Tapley Hill Formation (and base of the Farina Sub-Group).||||||
18197|Tindelpina Shale Member|24175|4|Described|p13|Neoproterozoic|Neoproterozoic|Basal facies of Tapley Hill Formation. Dark, finely laminated siltstone and dolomite.  Max. thickness: 80m.||||||13-FEB-08
18197|Tindelpina Shale Member|24176|4|Described|p12, p25 Tb. 1|Adelaidean|Adelaidean|Sequence of very finely laminated pyritic carbonaceous shale containing thin bands of live green limestone or dolomite. Of the Tapley Hill Formation.  Age is Sturtian. Geological Province: Mount Painter Province.||||||13-FEB-08
18197|Tindelpina Shale Member|24584|5|Briefly described|p14 Fig. 2|Neoproterozoic|Neoproterozoic|Carbonaceous shale.||||||
18197|Tindelpina Shale Member|29656|4|Described|Fig.3|||||||||
18197|Tindelpina Shale Member|29778|6|Mentioned|p167|||||||||
18197|Tindelpina Shale Member|29780|5|Briefly described|p35|||||||||
18197|Tindelpina Shale Member|29837|4|Described|p61|||||||||
18197|Tindelpina Shale Member|30052|6|Mentioned|Fig.5|||See also Fig.6. Proterozoic age.||||||
18197|Tindelpina Shale Member|30176|6|Mentioned|Map legend|Precambrian|Precambrian|Sturtian||||||
18197|Tindelpina Shale Member|30177|2|Defined|p129|Adelaidean|Adelaidean|Type areas: Approximately 2.4 miles north of Tindelpina Hut, lat. 30degrees04'56"S, long. 139degrees 19'02"E. Subsidiary type section: Sturt Gorge.||||||08-DEC-22
18197|Tindelpina Shale Member|30261|6|Mentioned|Table 1|||Sturtian - Marinoan||||||
18197|Tindelpina Shale Member|30713|5|Briefly described|p106|||||||||
18197|Tindelpina Shale Member|30801|6|Mentioned|p5|||Tapley Hill Formation. Table P5-6||||||
18197|Tindelpina Shale Member|30802|6|Mentioned|p12|||Sturtian age||||||
18197|Tindelpina Shale Member|30807|6|Mentioned|p103|||Suggested map symbol||||||
18197|Tindelpina Shale Member|30917|6|Mentioned|p36|||||||||
18197|Tindelpina Shale Member|31538|6|Mentioned|Fig. 1|||||||||
18197|Tindelpina Shale Member|32146|6|Mentioned|p346|||Points of interest for study||||||
18197|Tindelpina Shale Member|32506|6|Mentioned|p116|||||||||
18197|Tindelpina Shale Member|32510|6|Mentioned|Fig.1|||||||||
18197|Tindelpina Shale Member|32724|6|Mentioned|p509|||Sturtian. Lithology||||||
18197|Tindelpina Shale Member|33474|6|Mentioned|p540|||||||||
18197|Tindelpina Shale Member|34011|5|Briefly described|p67|||Sil.||||||
18197|Tindelpina Shale Member|34175|6|Mentioned|p36|||||||||
18197|Tindelpina Shale Member|34176|5|Briefly described|p51|||||||||
18197|Tindelpina Shale Member|34269|6|Mentioned|Table 1|||||||||
18197|Tindelpina Shale Member|34535|5|Briefly described|p66|||Sturtian-Marinoan. See Fig.22||||||
18197|Tindelpina Shale Member|34536|6|Mentioned|Map legend|Precambrian|Precambrian|Farina Sub-Gp.Sturtian||||||
18197|Tindelpina Shale Member|34587|6|Mentioned|p36|||||||||
18197|Tindelpina Shale Member|34812|6|Mentioned|p134|||||||||
18197|Tindelpina Shale Member|35255|6|Mentioned|Fig.6|||||||||
18197|Tindelpina Shale Member|35270|6|Mentioned|Fig.3|||||||||
18197|Tindelpina Shale Member|36126|6|Mentioned|Fig.1|||See also P1.||||||
18197|Tindelpina Shale Member|36837|6|Mentioned|p50|||||||||
18197|Tindelpina Shale Member|37932|5|Briefly described|p539|||||||||
18197|Tindelpina Shale Member|39344|6|Mentioned|Map legend|Precambrian|Precambrian|Sturtian||||||
18197|Tindelpina Shale Member|39348|6|Mentioned|Map legend|Precambrian|Precambrian|Sturtian||||||
18197|Tindelpina Shale Member|39635|6|Mentioned|Fig.7|||||||||
18197|Tindelpina Shale Member|40225|3|Fully described|Map sheet|||||||||
18197|Tindelpina Shale Member|40294|3|Fully described|p49|||See also p15.||||||14-MAY-07
18197|Tindelpina Shale Member|40442|6|Mentioned|p10|||||||||
18197|Tindelpina Shale Member|41405|3|Fully described|p165|||||||||
18197|Tindelpina Shale Member|41494|6|Mentioned|p35|||||||||
18197|Tindelpina Shale Member|42087|6|Mentioned|p17|||||||||
18197|Tindelpina Shale Member|42098|5|Briefly described|p53|||||||||
18197|Tindelpina Shale Member|42109|6|Mentioned|Table 1 P18|||||||||
18197|Tindelpina Shale Member|42222|5|Briefly described|p16|||||||||
18197|Tindelpina Shale Member|42238|6|Mentioned|p77|||||||||
18197|Tindelpina Shale Member|42720|5|Briefly described|map legend|Sturtian||||||||
18197|Tindelpina Shale Member|42813|5|Briefly described|p20|||Of Tapley Hill Formation.||||||13-FEB-08
18197|Tindelpina Shale Member|42882|5|Briefly described|Fig.4 P7|||of Tapley Hill Formation||||||
18197|Tindelpina Shale Member|43052|5|Briefly described|p186,Table 6.1|||Of Tapley Hill Formation.||||||13-FEB-08
18197|Tindelpina Shale Member|44659|5|Briefly described|map legend|||Marinoan, lithology.||||||
18197|Tindelpina Shale Member|44660|14|Not recorded|map legend|||Sturtian, lithology.||||||
18197|Tindelpina Shale Member|44689|14|Not recorded|map legend|||Andamooka. (H53-12).||||||
18197|Tindelpina Shale Member|50327|5|Briefly described|p306|Neoproterozoic|Neoproterozoic|Within the Adelaide Rift Complex of South Australia. Sturtian glacials. References to correlations with Tasmanian units.||||||07-FEB-11
18197|Tindelpina Shale Member|60718|5|Briefly described|p49 Fig. 2, p53, 55|Adelaidean|Adelaidean|Geological Province: Adelaide Geosyncline.||Of Tapley Hill Formation.||Gradationally(?) overlies Serle Conglomerate.|Black carbonaceous and pyritic deposit; contains thin interbeds of dolomite and thick-bedded conglomerate.|15-APR-11
18197|Tindelpina Shale Member|60955|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Of the Tapley Hill Formation. Finely-laminated carbonaceous shale.||||||
18197|Tindelpina Shale Member|60959|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Of the Tapley Hill Formation. Thinly laminated dolomicrite interbedded with siltstone and silty shale. Conglomerate bands.||||||
18197|Tindelpina Shale Member|61238|4|Described|p46 Fig. 2, p47 Fig. 3|Neoproterozoic|Neoproterozoic|Of the Umberatana Group. Shale, pyritic, carbonaceous, dolomite beds and lenses.||||||
18197|Tindelpina Shale Member|61732|5|Briefly described|p28 Fig. 13|Sturtian|Sturtian|Of the Tapley Hill Formation (Upalinna Subgroup, Umberatana Group). Geological Province: Adelaide Rift Complex.||||||07-FEB-11
18197|Tindelpina Shale Member|62903|5|Briefly described|p729, p730, p731|||Adelaide Rift Complex. End of Sturtian and Areyonga glaciations is constrained by Re-Os date of this unit that overlies the glaciation. The pooled Re-Os ages considered to be the best estimate of the depositional age of this unit. See also abbreviated Tindelpina Shale in this paper.|643.0+/-2.4 Ma Re-Os|base of Tapley Hill Formation||Tindelpina Shale Member (base of Tapley Hill Formation) overlies Yudnamutana Subgroup||
18197|Tindelpina Shale Member|64797|5|Briefly described|p153 Fig.2, p159, p163|||S-isotope data.||||||
18197|Tindelpina Shale Member|64846|5|Briefly described|p198-208 Fig.11, p212       |Cryogenian|Cryogenian|Carbon isotope details. Rank not shown in Fig.11.|643 +/- 2.4 Ma (Re-Os: Kendall et al.,2006)|Of the Tapley Hill Formation.||||
18197|Tindelpina Shale Member|65379|5|Briefly described|p643|Neoproterozoic|Neoproterozoic|Of Umberatana Group (Heyson Supergroup). Shale, pyritic, carbonaceous; thinly laminated grey dolomite beds and lenses. N.B. Asbestos deposit host.||||||07-MAR-12
18197|Tindelpina Shale Member|65493|5|Briefly described|p908, 910, 913, 917, Fig 2-6,16|Cryogenian|Cryogenian|At base of the Tapley Hill Formation, age: 643+/-2.4 Ma (Re-Os). Dark grey, pyritic dolomitic shale with regular interbeds of dolomite.||||||
18197|Tindelpina Shale Member|65925|5|Briefly described|Appendix 2.||||||||Shale, pyritic, carbonaceous; thinly laminated grey dolomite beds and lenses.|
18197|Tindelpina Shale Member|66884|5|Briefly described|p41 Fig.3|||Thickness: up to 25 m.||Umberatana Group|||Black shale, pyritic, carbonaceous with metre-scale dolomitic dropstones.|
18197|Tindelpina Shale Member|67030|5|Briefly described|p408|Cryogenian|Cryogenian|Age in conflict with age for Enorama Shale. Also spelt Tindelpina Shale member.|643 +/- 2.4 Ma (Re-Os, Kendell et al. 2006)|Of Tapley Hill Formation.||||26-APR-12
18197|Tindelpina Shale Member|67180|5|Briefly described|p600-02, p603 Fig.3, Fig. 4|Cryogenian|Cryogenian|Sturtian age. Approx. 80m thick in the Nepouie area. Beds grade upwards into thin silty and sandy dolomite interbeds separated by finely laminated shales. See also Tindelpena Shale. Shown to overlie the Serle Conglomerate Member of Preiss et al (1998).||Tapley Hill Formation, Nepouie Subgroup||Overlies the Merinjina Tillite; underlies the informal Siltstone Unit.|Finely laminated dolomites interbedded with non-calcareous shales. Dolomite interbeds most abundant at base, lowest beds bearing coarse clastic sand-cobble fragments in dolomicritic matrix. Passing (upwards) to very finely laminated shales.|
18197|Tindelpina Shale Member|67870|5|Briefly described|p24-25, p29-31, p33-35|Neoproterozoic|Neoproterozoic|Potential hydrocarbon source rocks: 2% TOC. Modelling suggests it is currently in the oil window. Detailed modelling showing fraction of kerogen transformed, and early oil and gas expulsion. Promoted to Group status [!] on p29-31, 32-34.||Tapley Hill Formation.|||Organic rich shale and limestone.|
18197|Tindelpina Shale Member|67979|4|Described|p529-532, p537-8, p541-2, Figs.3,5,6,7|Sturtian|Bolindian|The regional basal dolomitic facies is recognised as the post-Sturtian glaciation cap carbonate (Giddings and Wallace 2009a). Type section at Tindelpina Hut is not typical. It is  missing the lower laminated carbonate facies . Thickness: 280 m at Tindelpina Hut section. Transitionally (conformably) overlies Serle Conglomerate Member (base of Tapley Hill Formation at Tindelpina Hut section).  Also on p545,  Figs. 6, 7, 8. 11.||Base of Tapley Hill Formation.||Abruptly overlies Bolla Bollana Formation (Yudnamutana section) and Merinjina Tillite (Illinawortina section); conformably overlies Wilyerpa Formation. See comments.|Regionally finely laminated dolomites gradationally overlain by very fine-grained dolomitic shales; only at Tindelpina type area, boulder and pebble conglomerates interbedded within fine-grained calcareous shales.|22-SEP-14
18197|Tindelpina Shale Member|68030|6|Mentioned|p236|||Flinders Ranges. Carbonaceous, calcareous and pyritic deposit that caps the Fe-rich diamictite and tillite formations of the Sturt Glaciation.||Unit of Tapley Hill Formation.||||
18197|Tindelpina Shale Member|68243|6|Mentioned|p654|Cryogenian|Cryogenian||ca. 643 +/- 2 Ma, Re-Os.|||||
18197|Tindelpina Shale Member|68244|6|Mentioned|p671||||643+\-2.4 Ma||||Black shales.|
18197|Tindelpina Shale Member|68270|5|Briefly described|p683|Cryogenian|Cryogenian|Adelaide Rift Complex. 647.2+\-10 Ma and 645.1+\-4.8 Ma, Tindelpina Shale Member (Kendall et al. 2006).||Unit of Umberatana Group.||||
18197|Tindelpina Shale Member|69019|5|Briefly described|p47.|Neoproterozoic|Neoproterozoic|Regionally extensive, but does not occur in this map area.||Basal unit in Tapley Hill Formation.|||Dark grey pyritic shale and dolomite.|
18197|Tindelpina Shale Member|69666|5|Briefly described|p33|Neoproterozoic|Neoproterozoic|Adelaide Geosyncline and Stuart Shelf.|643 +/- 2.4 Ma (Re-Os: Kendall et al., 2006).|Tapley Hill Formation.||||
18197|Tindelpina Shale Member|69873|5|Briefly described|p82-83|||Adelaide Rift Complex. Included in diagram showing Cryogenian-Ediacaran stratigraphy and correlations with Tasmanian succession. Abbreviated to Tindelpina Shale on p83.|647 +/- 10 Ma; 645 +/- 5 Ma (Kendall et al. 2006)|Unit in Umberatana Group.||Correlated with Julius River Member (Tas).||
18197|Tindelpina Shale Member|70031|4|Described|p245-246|Cryogenian|Cryogenian|Adelaide Geosyncline. Lower interglacial succession; waning stages of Sturtian glaciation. Thickness: ~60m. Represents a 'cap carbonate' overlying Sturt glaciation deposits at a sequence boundary. Re-Os diagenetic age of black shales at 643.0+\-2.4 Ma (Kendall et al., 2006).|643.0+\-2.4 Ma|Unit of Tapley Hill Formation.||Overlain conformably by Tapley Hill Formation. Underlain by Wilyerpa Formation/Yudnamutana Subgroup.|Dark grey to black, thinly laminated, pyritic, carbonaceous siltstone and dolostone.|
18197|Tindelpina Shale Member|70082|6|Mentioned|p2-3|Cryogenian|Cryogenian|Flinders Ranges. Contains Re-Os age of 643+\- 2.4 Ma (Kendall et al., 2009).||Unit of Tapley Hill Formation.||||
18197|Tindelpina Shale Member|70334|6|Mentioned|p48|||||||||
18197|Tindelpina Shale Member|70384|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Adelaide Geosyncline. Age shown more specifically as Sturtian [Cryogenian].||Of Tapley Hill Formation.||Overlies Serle Conglomerate.|Pyritic, carbonaceous shale; thinly laminated grey dolomite beds and lenses.|23-JAN-19
18197|Tindelpina Shale Member|70819|6|Mentioned|p29|Neoproterozoic|Neoproterozoic|Clare Valley.|643 +/- 2.4 Ma (Re-Os; Kendall et al., 2006).|Tapley Hill Formation.||||
18197|Tindelpina Shale Member|71129|5|Briefly described|p108,110|Cryogenian|Cryogenian|Of Adelaide Geosyncline. Contains Re-Os age of 643+\-2.5 Ma of organic matter (Kendall et al., 2006).||Basal unit of Tapley Hill Formation.||Correlable with Lincoln Member.||13-NOV-19
18197|Tindelpina Shale Member|71895|6|Mentioned|APP4. p4, APP8. p201-p203|||Punt Hill Region.||||||
18197|Tindelpina Shale Member|72450|5|Briefly described|Brochure map|||||Umberatana Group|||Laminated, pyritic, black shale and dolomite.|
18197|Tindelpina Shale Member|72473|6|Mentioned|p4-5|||Thickness: ca 60 m. Considered to be a 'cap dolomite'. Often sharply defined by thin, continuous dolomite bands that conformably overlie the diamictites, siltstones and sandstones of the Sturtian glacial deposits.||Tapley Hill Formation|||Dark grey, pyritic, carbonaceous, or dolomitic silty shale.|
18197|Tindelpina Shale Member|72601|6|Mentioned|p6|Cryogenian|Cryogenian||643 +/- 2.4 Ma [Re-Os?]|Tapley Hill Formation, Umberatana Group||||
18197|Tindelpina Shale Member|72613|5|Briefly described|p2,  p3 Fig 2|Cryogenian|Cryogenian|Shown as Sturtian age. Includes the 'cap dolostone' of the Sturtian glaciation.||Of Tapley Hill Formation||Conformably overlies the Yudnamutana Subgroup. Overlies Merinjina Diamictite.||
18197|Tindelpina Shale Member|73110|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|||Tapley Hill Formation.|||Shale, pyritic, carbonaceous; thinly laminated grey dolomite beds and lenses.|
18197|Tindelpina Shale Member|74367|5|Briefly described|p7 Fig.6, p8, p11, p19|Cryogenian|Crogenian|See also Tindelpina Shale p19.|643+/-2.4 Ma Re-Os whole rock|Tapley Hill Formation, basal part|||Black shales.|
18222|Tintinara Granite|42549|5|Briefly described|p158|||||||||
18227|Tirari Formation|23155|6|Mentioned|p36|||||||||
18227|Tirari Formation|24175|5|Briefly described|p42, p32 Fig. 6|Quaternary|Late Pliocene|Age: >440 000B.P (G.C. Nanson, Univ. Wollongong, pers. comm., 1991).  Geological Province: Lake Eyre Basin.||||||
18227|Tirari Formation|30056|6|Mentioned|p148|||||||||
18227|Tirari Formation|30061|6|Mentioned|p11|||||||||
18227|Tirari Formation|30804|5|Briefly described|p13|||On Table 1||||||
18227|Tirari Formation|30807|6|Mentioned|p101|||Suggested map symbol||||||
18227|Tirari Formation|30919|6|Mentioned|Map legend|Quaternary|Quaternary|||||||
18227|Tirari Formation|30920|6|Mentioned|Map legend|Pleistocene|Pleistocene|? Equivalent Eurinella Formation||||||
18227|Tirari Formation|31532|6|Mentioned|Table 1|||||||||
18227|Tirari Formation|31699|4|Described|p132|||?Pleistocene or ?Pliocene||||||
18227|Tirari Formation|33820|6|Mentioned|Map legend|Pleistocene|Pliocene|Pliocene - Pleistocene||||||
18227|Tirari Formation|33821|6|Mentioned|Map legend|Pleistocene|Pliocene|Pliocene - Pleistocene||||||
18227|Tirari Formation|33822|6|Mentioned|Map legend|Pleistocene|Pliocene|Pliocene to Pleistocene||||||
18227|Tirari Formation|33823|6|Mentioned|Map legend|Pleistocene|Pliocene|Pliocene - Pleistocene||||||
18227|Tirari Formation|33824|6|Mentioned|Table 2|||||||||
18227|Tirari Formation|33825|6|Mentioned|p7|||Correlation||||||
18227|Tirari Formation|33827|6|Mentioned|Table 1|||||||||
18227|Tirari Formation|33828|6|Mentioned|p11|||||||||
18227|Tirari Formation|33831|6|Mentioned|Map legend|Pleistocene|Pliocene|Pliocene - Pleistocene||||||
18227|Tirari Formation|33832|6|Mentioned|p6|||Stratigraphy||||||
18227|Tirari Formation|34308|6|Mentioned|p200|||Late Tertiary||||||
18227|Tirari Formation|35691|6|Mentioned|p5|||||||||
18227|Tirari Formation|36213|6|Mentioned|Fig.2|||||||||
18227|Tirari Formation|40755|5|Briefly described|App.3.1|||||||||
18227|Tirari Formation|40756|5|Briefly described|p3|||||||||
18227|Tirari Formation|40757|6|Mentioned|p78|||||||||
18227|Tirari Formation|40926|6|Mentioned|Table 3|||||||||
18227|Tirari Formation|41206|5|Briefly described|p371|||||||||
18227|Tirari Formation|41257|5|Briefly described|p4|||||||||
18227|Tirari Formation|41537|6|Mentioned|p350|||See also Fig.2||||||
18227|Tirari Formation|42090|6|Mentioned|p43|||||||||
18227|Tirari Formation|42124|6|Mentioned|p43|||||||||
18227|Tirari Formation|42375|4|Described|p43-44|||Lake Eyre Basin Defined Stirton 1961.||||||
18227|Tirari Formation|42457|6|Mentioned|p161|||near Lake Eyre||||||
18227|Tirari Formation|42477|5|Briefly described|p186|||||||||
18227|Tirari Formation|42592|5|Briefly described|Fig. 6 P272, P273|||Type locality indicated||||||
18227|Tirari Formation|42746|5|Briefly described|p22|||See also Fig.2 P4.||||||
18227|Tirari Formation|42784|6|Mentioned|p494|||||||||
18227|Tirari Formation|43041|5|Briefly described|Fig.1,p590|||||||||
18227|Tirari Formation|44133|5|Briefly described|p244 Table 11.3, 190 Fig. 10.30, 194|Pleistocene|Pliocene|Geoloigcal Province: Lake Eyre Basin. Maximum Thickness: 12m.||||||
18227|Tirari Formation|44223|14|Not recorded|p.157,158|||Unfossiliferous. Overlies Pliocene Mampuwordu Sands; Underlies Pliestocene Katipiri Sands.||||||
18227|Tirari Formation|44228|14|Not recorded|p.131|||||||||
18227|Tirari Formation|44238|14|Not recorded|Fig.3|Pleistocene|Pliocene|Pliocene-Pleistocene.||||||
18227|Tirari Formation|45128|6|Mentioned|p61|||||||||
18227|Tirari Formation|60703|5|Briefly described|p704 Fig. 2, p725 Fig.18|Pliocene|Pliocene|Geological Province: Lake Eyre Basin.||||||12-APR-05
18227|Tirari Formation|60953|5|Briefly described|Map Legend|Pleistocene|Pliocene|Fluvial and fluviolacustrine sediments.||||||
18227|Tirari Formation|61108|5|Briefly described|map legend|Pleistocene|Pliocene|Fluvial and fluviolacustrine sediments: channel sand, clay, some vertebrate fossils; often gypsified.||||||01-JUN-05
18227|Tirari Formation|61155|5|Briefly described|p5, p17|Late Pliocene|Early Pliocene|Fluvial sandy deposits near Lake Eyre. Overlies the Mampuwordu Sand. Age: 3.5-1.5Ma. Geological Province: Lake Eyre Basin.||||||
18227|Tirari Formation|66131|5|Briefly described|p240, p242 Fig.2, p244-p246, p257|Pliocene|Pliocene|~4-5m thick. Dated using thermoluminescence. Contains fossils of Diprotodon and short-faced kangaroos.|> 0.4 Ma|||Overlies Wipajiri Formation. Contains channel fills of the Kutjitara Formation.|Widespread, red-brown silt with sandy channel deposits, usually cemented with massive gypcrete.|
18227|Tirari Formation|66573|5|Briefly described|p873-876, p881; Tb.2, Fig. 4, Fig.15|Pliocene|Pliocene|Overlies the Mampuwordu Sand; is overlain unconformably by Kutjitara Formation and Katipiri Sands. Red sandstones and claystones with gypsum beds.||||||
18227|Tirari Formation|67462|5|Briefly described|Map legend.|Pleistocene|Pliocene|Tirari Sub-basin, Lake Eyre Basin.||||||
18227|Tirari Formation|68715|6|Mentioned|p30 Fig.5|Piacenzian|Zanclean|Tirai and northern Callabonna sub basins, Lake Eyre Basin.||||||
18227|Tirari Formation|69019|6|Mentioned|p105 Fig.25.|Pliocene|Pliocene|Tirari Sub-basin.||||||
18227|Tirari Formation|69023|5|Briefly described|p108, p124|Pliocene|Pliocene|Tirari Sub-basin, Lake Eyre Basin. Probably partly equivalent to Yandruwantha Sand.||||||
18227|Tirari Formation|70823|5|Briefly described|p47|||Lake Eyre Basin.|||||Red and yellow sand and sandy clay.|
18232|Tirrawarra Sandstone|13497|3|Fully described|iv, vi, viii, x, xii, p47-p48, |Asselian|Stephanian|Cooper Basin. Previously the Tirrawarra Formation of Kapel (1972) before being renamed by Gatehouse in the same year. The name is derived from the Tirrawarra Swamp. A reference section is mentioned. This formation is widespread but thin, only reaching 75m thick. Hosts the largest Permian oil accumulation in the Cooper Basin. Deposited in a braidplain or deltal environment. Reservoir characteristics discussed. See also p54, p61, p64-p66, p69 fig 6.1, p75-p78, p81, p84-90, p119, p122, p138 fig 8.17, p139 fig 8.18, p141, p146,  p150, p153,  p157-p160, p173, p177, p181-p184, p188-p190, p204, p208, p216.||Gidgealpa Group||Interfingers with or unconformably overlies the Merrimelia Formation. Interfingers with and is overlain by the Patchawarra Formation.|Brown and white, fine to coarse-grained, moderately well sorted sandstone with minor shale interbeds and rare thin coal seams and stringers.|
18232|Tirrawarra Sandstone|13516|6|Mentioned|p147, fig 5|Early Permian|Early Permian|From Cooper Basin||||||
18232|Tirrawarra Sandstone|22527|4|Described|p 2, 3, 4,||Early Permian|Replaced by Big Lake Suite, in Moomba Field.  Informally termed "Tirrawarra Conglomerate".||||||14-APR-08
18232|Tirrawarra Sandstone|22839|6|Mentioned|P33|||||||||
18232|Tirrawarra Sandstone|22883|6|Mentioned|P29|||Underlying unit is Merrimelia Formation||||||
18232|Tirrawarra Sandstone|23154|5|Briefly described|Map Legend|Early Permian|Early Permian|Geological Province - Cooper Basin.  Parent - Gidgealpa Group.||||||
18232|Tirrawarra Sandstone|23155|4|Described|p14 & p17|Early Permian|Late Carboniferous|Sparse spore-pollen assemblages indicate that the unit is predominantly Early Permian in age but may range downward into the Late Carboniferous where interbedded with the Merrimelia Formation.  Thickness distribution in the unit is variable (see p 17).||||||
18232|Tirrawarra Sandstone|23375|4|Described|Fig2 p265,285||Asselian|In the Cooper Basin.||||||17-JAN-08
18232|Tirrawarra Sandstone|24199|5|Briefly described|p512 Fig.2|Early Permian|Early Permian|Geological Province: Cooper Basin.||||||
18232|Tirrawarra Sandstone|24204|5|Briefly described|p262, 263 Fig.4, p284|Early Permian|Early Permian|Mainly discussed in terms of Tirrawarra Sandstone equivalent. Geological Province: Cooper Basin.||||||31-MAR-05
18232|Tirrawarra Sandstone|24212|5|Briefly described|p67 Fig. 3p|Early Permian|Early Permian|Age: >290Ma.  Geological Province: Cooper Basin.||||||
18232|Tirrawarra Sandstone|29387|6|Mentioned|Table 2|||Refers to Gatehouse 1972.||||||
18232|Tirrawarra Sandstone|29721|6|Mentioned|Table 137|||||||||
18232|Tirrawarra Sandstone|30540|6|Mentioned|p65|||Produces gas in Gidgealpa No.7||||||
18232|Tirrawarra Sandstone|30544|6|Mentioned|p53|||||||||
18232|Tirrawarra Sandstone|30873|3|Fully described|p14|||Refers Kapel (1972). Previously Tirrawarra Formation.||||||30-JUN-08
18232|Tirrawarra Sandstone|32696|6|Mentioned|Fig.4|||Refers Gatehouse (1972)||||||
18232|Tirrawarra Sandstone|33074|6|Mentioned|p260|||||||||
18232|Tirrawarra Sandstone|33331|6|Mentioned|p41|||||||||
18232|Tirrawarra Sandstone|33489|6|Mentioned|Fig.2|||Refers Kapel (1972) & Gatehouse (1972)||||||
18232|Tirrawarra Sandstone|35067|6|Mentioned|Fig.4|||||||||
18232|Tirrawarra Sandstone|35068|6|Mentioned|Fig.3|||Discussed P54.||||||
18232|Tirrawarra Sandstone|35457|6|Mentioned|Fig.4|||Biostratigraphic relationships. See also P627.||||||
18232|Tirrawarra Sandstone|35573|6|Mentioned|Fig.7|||Generalised stratigraphy - Southern Cooper Basin||||||
18232|Tirrawarra Sandstone|35845|4|Described|p24|||Lithology and depositional environments. See also p42.||||||17-JAN-08
18232|Tirrawarra Sandstone|36099|6|Mentioned|p191|||||||||
18232|Tirrawarra Sandstone|36910|6|Mentioned|Fig.4|||||||||
18232|Tirrawarra Sandstone|36917|6|Mentioned|Fig.1|||||||||
18232|Tirrawarra Sandstone|37703|6|Mentioned|p2240|||||||||
18232|Tirrawarra Sandstone|37855|6|Mentioned|p4|||See also Fig.2.||||||
18232|Tirrawarra Sandstone|37917|6|Mentioned|Fig.2|||||||||
18232|Tirrawarra Sandstone|38977|6|Mentioned|Fig.1|||||||||
18232|Tirrawarra Sandstone|39252|5|Briefly described|p13|||||||||
18232|Tirrawarra Sandstone|39254|5|Briefly described|p45|||||||||
18232|Tirrawarra Sandstone|39261|6|Mentioned|Fig. 9|||||||||
18232|Tirrawarra Sandstone|39265|6|Mentioned|Fig. 3|||||||||
18232|Tirrawarra Sandstone|39276|6|Mentioned|Fig. 2|||||||||
18232|Tirrawarra Sandstone|39445|5|Briefly described|Table 7|||See also P92 & Table 8||||||
18232|Tirrawarra Sandstone|39478|6|Mentioned|Table 1|||||||||
18232|Tirrawarra Sandstone|39494|6|Mentioned|Fig.3|||||||||
18232|Tirrawarra Sandstone|40030|6|Mentioned|p131|||See also Fig.3||||||
18232|Tirrawarra Sandstone|40249|6|Mentioned|p45|||||||||
18232|Tirrawarra Sandstone|40544|6|Mentioned|Fig.4|||||||||
18232|Tirrawarra Sandstone|41099|6|Mentioned|p190|||||||||
18232|Tirrawarra Sandstone|41123|6|Mentioned|p180|||||||||
18232|Tirrawarra Sandstone|41131|6|Mentioned|Fig.3|||||||||
18232|Tirrawarra Sandstone|41164|6|Mentioned|Table 1|||||||||
18232|Tirrawarra Sandstone|41166|4|Described|p379|||||||||
18232|Tirrawarra Sandstone|41183|6|Mentioned|p307|||See also Fig.3||||||
18232|Tirrawarra Sandstone|41189|6|Mentioned|Fig.4|||||||||
18232|Tirrawarra Sandstone|41198|6|Mentioned|Table 1|||||||||
18232|Tirrawarra Sandstone|41214|6|Mentioned|Fig.3|||||||||
18232|Tirrawarra Sandstone|41221|6|Mentioned|p389|||||||||
18232|Tirrawarra Sandstone|41247|6|Mentioned|Fig.5|||||||||
18232|Tirrawarra Sandstone|41267|6|Mentioned|p262|||||||||
18232|Tirrawarra Sandstone|41288|6|Mentioned|p156|||||||||
18232|Tirrawarra Sandstone|41595|6|Mentioned|Fig. 5|||||||||
18232|Tirrawarra Sandstone|41720|6|Mentioned|p370|||||||||
18232|Tirrawarra Sandstone|42085|6|Mentioned|Fig.2 P374|||||||||
18232|Tirrawarra Sandstone|42395|5|Briefly described|Fig.13 P83|||||||||
18232|Tirrawarra Sandstone|42547|4|Described|p81|||||||||
18232|Tirrawarra Sandstone|42746|5|Briefly described|p3|||Cooper Basin||||||
18232|Tirrawarra Sandstone|42999|5|Briefly described|Table 2,p90||Early Permian|||||||
18232|Tirrawarra Sandstone|43018|5|Briefly described|Table 1,p386|||||||||
18232|Tirrawarra Sandstone|43105|5|Briefly described|Fig.7,p13.|||||||||
18232|Tirrawarra Sandstone|43570|5|Briefly described|Fig.2,p535,541|Early Permian|Late Carboniferous|||||||
18232|Tirrawarra Sandstone|43628|6|Mentioned|Fig.3||Early Permian|||||||
18232|Tirrawarra Sandstone|43711|6|Mentioned|p19||Early Permian|||||||
18232|Tirrawarra Sandstone|44133|4|Described|p65 Fig. 8.3, 83, 84|Sakmarian|Asselian|Of the Gidgealpa Group. Geological Province: Cooper Basin. Average Thickness: ~70m. Conformably underlies Patchawarra Formation.||||||
18232|Tirrawarra Sandstone|46849|6|Mentioned|Fig. 7|||||||||
18232|Tirrawarra Sandstone|48995|6|Mentioned|Fig.3|||||||||
18232|Tirrawarra Sandstone|60386|6|Mentioned|p296|Sakmarian|Sakmarian|Cooper Basin. Non-marine.||||||
18232|Tirrawarra Sandstone|60717|5|Briefly described|p40 Fig. 2, p41|Asselian|Late Carboniferous|Probably supersedes Tirrawarra Formation? Of the Gidgealpa Group. Thickness: 75m. Geological Province: Cooper Basin.||||||31-JAN-08
18232|Tirrawarra Sandstone|61015|6|Mentioned|p44|||In the Cooper-Eromanga Basins.||||||
18232|Tirrawarra Sandstone|61250|6|Mentioned|p45|||Contains petroleum systems. Geological Province: Cooper Basin.||||||
18232|Tirrawarra Sandstone|61614|6|Mentioned|p290, p294, p295, p290 Fig. 2|||Of Gidgealpa Group. Geological Province: Cooper Basin.||||||17-MAR-09
18232|Tirrawarra Sandstone|61615|5|Briefly described|p302, p303, p302 Fig. 2|Early Permian|Late Carboniferous|Of Gidgealpa Group. Overlain by Patchawarra Formation. Geological Province: Cooper Basin. Glacial or braided fluvial deposits.||||||22-AUG-18
18232|Tirrawarra Sandstone|61616|6|Mentioned|p330 Fig. 2|Early Permian|Late Carboniferous|Of Gidgealpa Group. Geological Province: Cooper Basin.||||||31-MAR-09
18232|Tirrawarra Sandstone|62046|5|Briefly described|p125 Fig. 2|Permian|Carboniferous|Geological Province: Cooper-Eromanga Basins.||||||14-APR-08
18232|Tirrawarra Sandstone|62376|5|Briefly described|p84|Early Permian|Late Carboniferous|Geological Province: Pedirka Basin.||||||09-FEB-10
18232|Tirrawarra Sandstone|62537|6|Mentioned|p191 Fig.2. |Early Permian||Cooper Basin.||Unit in Gidgealpa Group.||Overlies Merrimelia Formation. Is overlain by Patchawarra Formation.||
18232|Tirrawarra Sandstone|62730|5|Briefly described|p352 Fig. 1|Early Permian|Late Carboniferous|Geological Province: Cooper Basin.||||||14-APR-08
18232|Tirrawarra Sandstone|62759|5|Briefly described|p1|||Geological Province: Cooper Basin. Correlates with a glacigene sandstone at base of Purni Formation in the Perdika Basin.||||||05-FEB-08
18232|Tirrawarra Sandstone|63832|5|Briefly described|p131 fig 2, p135|Cisuralian|Cisuralian|Of Cooper Basin. Is mentioned on p135 as the abbreviated [and mis-spelt] Tirrawarra-Merimelia Formations. Thick succession of continental proglacial and possibly subglacial facies.||||Overlies and interfingers with Merrimelia Formation.|Continental proglacial and possibly subglacial facies.|14-DEC-17
18232|Tirrawarra Sandstone|63978|2|Defined|p10, Fig. 3|Early Permian|Early Permian|Of Gidgealpa Gp.Conformable over Merrimelia Fm; conformable under Patchawarra Fm; intertongues with both. Thick: 44m. Mainly fine- to coarse-gr.+ pebbly sandstone (massive)+ interbeds of conglomerate+ minor interbeds of carbonaceous siltst, shale+coal||||||07-FEB-11
18232|Tirrawarra Sandstone|64048|5|Briefly described|p65|Early Permian|Early Permian|Contains very small reserves of oil.||||||07-FEB-11
18232|Tirrawarra Sandstone|64197|6|Mentioned|p625 Fig.1c|Permian|Carboniferous|Cooper Basin.||||Underlies the Patchawarra Formation, overlies the Merrimelia Formation.||
18232|Tirrawarra Sandstone|64631|5|Briefly described|p44 Fig.2, p49.|Sakmarian|Asselian|Cooper Basin. Contains thick successions of continental proglacial facies. Some biostratigraphic age control. Shown with time transgressive base.||||Overlies Merrimelia Formation. Overlain by Patchawarra Sandstone.||
18232|Tirrawarra Sandstone|64665|5|Briefly described|p53 Fig.2, p56.|Early Permian|Early Permian|Cooper Basin. Hydrocarbon reservoirs are thought to have been charged from Patchawarra Formation.||||Overlies Merrimelia Formation. Is overlain by Patchawarra Formation.||
18232|Tirrawarra Sandstone|64778|6|Mentioned|p13|Carboniferous|Carboniferous|Pedirka Basin.||||||
18232|Tirrawarra Sandstone|65238|5|Briefly described|p3, p5 Fig. 6, p7 Fig. 8|Early Permian|Late Carboniferous|Geological province: Pedirka Basin, Cooper Basin. Glacial outwash deposits.||||||09-APR-13
18232|Tirrawarra Sandstone|65489|5|Briefly described|p11, p15-16, p47-49, p55, p96, p131-132|Asselian|Late Carboniferous|See also p143. Cooper Basin. 75m thick. In 1970 Bridge Oil announced flow of light crude oil from Tirrawarra 1. Gas and oil reservoir accounting for 6% and 90% respectively of the Basin's production.||Unit in Gidgealpa Group.||Overlies Merrimelia Formation. Is overlain by Patchawarra Formation.|Braided fluvial to fan-delta deposits.|
18232|Tirrawarra Sandstone|65925|5|Briefly described|Appendix 2.||||||||Conglomerate, medium- to coarse-grained sandstone, mudstone; minor coal.|
18232|Tirrawarra Sandstone|67402|5|Briefly described|p90, p90 fig CPR4|||Deposited by high energy braided fluvial system and associated outwash fan deposits. See also p91 tbl CPR1, p99 fig CPR14, p101, p101 tbl CPR2, p104.||Gidgealpa Group||Overlies the Merrimelia Formation. Overlain by the Patchawarra Formation.|Fine-grained to pebbly, massive to planar cross-bedded sandstone with common beds of conglomerate, carbonaceous siltstone, shale and coal.|
18232|Tirrawarra Sandstone|68731|5|Briefly described|p200 Fig 3.110, p204, p205, p206|Cisuralian||(Kapel 1972; Gatehouse 1972). ~ 40 m thick. Deposited by melt-water streams flowing north from retreating glaciers as reworked unconsolidated glacial sediments and has yielded Cisuralian palynofloras.||Of the Gidgealpa Group.||Interdigitated with the Merrimelia Formation. Overlain by the Patchawarra Formation. Conformably underlain by the Merrimelia Formation.|Comprises fine to coarse and pebbly sandstone, with common conglomerates and minor carbonaceous siltstone, shale, and coal. Sandstone is massive, with flat or planar cross-bedding and a siliceous or kaolinitic matrix.|12-MAY-16
18232|Tirrawarra Sandstone|69023|4|Described|p79, p81, p82 Fig.18, p83, p191-192|Permian|Late Carboniferous|Cooper Basin. A more recent addition to the Gidgealpa Group: was recognised by Kapel (1972) and Gatehouse (1972). Gas reserves. Fluvio-glacial. Incorrectly labelled as Tirrawarra Formation on the CALLABONNA map reference. 54.9 to 69.5m thick. Stratigraphic wells intersection data.||Unit in Gidgealpa Group.||Overlies and interbedded with  Merrimelia Formation. Is overlain by Patchawarra Formation.|Buff-white to brownish, medium- to coarse-grained sandstone; massive to flat-bedded and cross-bedded, with a siliceous or kaolinitic matrix; rare pebbly sandstone to conglomerate; scarce carbonaceous mudstone and coal stringers.|
18232|Tirrawarra Sandstone|69454|4|Described|p38:3-4, 6-7, 12-13, 14 Fig.38.9|Sakmarian|Asselian|McKellar (2002). Defined in the Cooper Basin in SA and Qld. Rocks in the Pedirka Basin are referred to as 'Tirrawarra Sandstone equivalent', and were included as upper Crown Point Formation by Jones et al. (2011). 200m thick in Mount Hammersley-1. Glaciofluvial braided river/glacial outwash deposits. Has fair to good reservoir potential, sealed by basal Purni Formation shale (in the Pedirka Basin) or Patchawarra Formation (in the Cooper Basin).||||Conformably overlies and interfingers with Crown Point Formation. Is overlain conformably by Purni Formation.|Very fine to very coarse to conglomeratic feldspathic sandstone; minor siltstone and claystone.|22-AUG-18
18232|Tirrawarra Sandstone|69457|6|Mentioned|p41:5 Fig.41.4|||||||||12-JUL-16
18232|Tirrawarra Sandstone|69673|6|Mentioned|p149, p150, p151, p160|||||||Overlain by Purni Formation|Sandstone, conglomerate and lesser siltstone.|
18232|Tirrawarra Sandstone|69797|5|Briefly described|p17 Fig.2|Early Permian|Late Carbonfierous|Age: Stephanian - Asselian (approximated from figure). Geol. Prov: Cooper Basin.||Gidgealpa Group||||
18232|Tirrawarra Sandstone|69946|5|Briefly described|p3, p9, p36, p45, p54|Sakmarian|Asselian|Southern Cooper Basin. Braided fluvial to proglacial outwash deposits.||||Overlies Merrimelia Formation. Is overlain by Patchawarra Formation. Equivalent to Boorthanna Formation (Arckaringa Basin).||
18232|Tirrawarra Sandstone|69947|5|Briefly described|p13 Fig.7.2|Permian|Late Carboniferous|Cooper Basin.||Gidgealpa Group.||||
18232|Tirrawarra Sandstone|69982|5|Briefly described|p13, p44, Appendix 1|Permian|Permian|Cooper Basin. Hydrocarbon shows from the Warburton Basin rocks have been incorrectly assigned to this unit (and others). Brief thin section descriptions. Appears as "Tirrawarra sandstone" on p103.||||||
18232|Tirrawarra Sandstone|70317|6|Mentioned|p33, 36|Early Permian|Late Carboniferous|Cooper Basin. Vertical section showing fracture densities.||Gidgealpa Group.||Overlies Merrimelia Formation, locally unconformably. Is overlain by Patchawarra Formation.||
18232|Tirrawarra Sandstone|70823|4|Described|iv, p25-p27, p36, 51-53|Asselian|Pennsylvanian|Cooper Basin. Up to 75m thick. Deposited in a proglacial outwash or braided fluvial environment. Some debate about age. Palynofloras are consistent with APP1.21, 1.22 and basal APP21.palynological zones. Hosts a commercial oil reservoir that is briefly discussed. See also p40-p41, p78-p80, p82.||Gidgealpa Group||Overlies and interfingers with the Merrimelia Formation. Overlain by and interfingers with the Patchawarra Formation.|Fine to coarse-grained, moderately well sorted sandstone, common conglomerates with minor shale interbeds and rare thin coal seams and stringers.|22-AUG-18
18232|Tirrawarra Sandstone|70824|4|Described|p7-p9, p38, p43-p47, p122|Asselian|Gzhelian|Cooper Basin. Up to 75m thick. Deposited as proglacial outwash or in a braided fluvial environment. Outcrop and areal extent briefly discussed.||||Conformably overlies the Merrimelia Formation. Overlain by the Patchawarra Formation.|Fine to coarse-grained, moderately well sorted sandstone, common conglomerates with minor shale interbeds and rare thin coal seams and stringers.|
18232|Tirrawarra Sandstone|70946|5|Briefly described|p1089|Permian|Carboniferous|Cooper Basin. Deposited in a proglacial outwash or braided fluvial environment.||Gidgealpa Group.||||08-OCT-18
18232|Tirrawarra Sandstone|71265|5|Briefly described|p589|Asselian|Asselian|Cooper Basin.||Gidgealpa Group.||Overlies Merrimelia Formation. Is overlain by Patchawarra Formation.||
18232|Tirrawarra Sandstone|71342|5|Briefly described|Ch5 p3, Ch5 p9, Ch5 p36, Ch5 p45|Sakmarian|Asselian|Cooper Basin. Deposited in a braided fluvial to proglacial outwash environment. Palynological zone is given in fig 5.3 Ch5 p36. Thermal history briefly described in Ch9. See also Ch5 p54, Ch7 p13, Ch9 p5, Ch9 p10-p11, Ch10 tbl 10.1, Ch10 p7, Ch10 p13-p14, Ch10 p17, Ch10 p19-p20, Ch11 p8, Ch13 p9.||Gidgealpa Group||Overlies the Merrimelia Formation. Overlain by the Patchawarra Formation.||
18232|Tirrawarra Sandstone|71701|5|Briefly described|p155|Asselian|Gzhelian|Cooper Basin.||Gidgealpa Group||Overlies the Merrimelia Formation. Overlain by the Patchawarra Formation.||
18232|Tirrawarra Sandstone|72297|5|Briefly described|p742|||Cooper Basin. Contains minor oil reserves at Pepita, and has some reservoir potential. [Next paragraph]: The largest onshore Permian oilfield in Australia is reservoired in the Tirrawarra Sandstone.||||||
18232|Tirrawarra Sandstone|72497|5|Briefly described|p13, p17 Fig.11.|Early Permian|Late Carboniferous|Cooper Basin. Described as fluvioglacial outwash deposits and overlying braided stream environment .||||Overlies Merrimelia Formation with diachronous contact?||
18232|Tirrawarra Sandstone|73251|6|Mentioned|p62|Cisuralian|Late Carboniferous|Cooper Basin. Proglacial outwash and braided fluvial depositional environments. Contains[?] gas and oil.||Gidgealpa Group||Underlain by Merrimelia Formation. Overlain by Patchawarra Formation.||
18232|Tirrawarra Sandstone|73281|6|Mentioned|Appendix (DIP)|||See DIP034_Petroleumdata.xlsx and DIP034_Welldata.xlsx.||||||
18232|Tirrawarra Sandstone|73495|5|Briefly described|p497, p499, p503-504, p506|||Cooper Basin. Top contact may represent an unconformity. Reflects a braided fluvioglacial to fluvial setting with floodplains and rare mires.||||Underlain by and interfingering with Merrimelia Formation. Overlain by the Patchawarra Formation.|Locally developed conglomerate beds, fine- to coarse-grained and moderately to well-sorted sandstones (sublitharenites), minor shales and rare, thin coal beds.|
18357|Toolachee Formation|13497|3|Fully described|iv, v, vi, viii, x, xi|Late Permian|Late Permian|Cooper Basin. Named by Kapel (1972) and defined by Gatehouse (1972). Morton and Gatehouse (1985) redefined the formation to exclude parts of the Daralingie Formation included in the type section. A type section is briefly mentioned. Petrography and fossil assemblage is discussed in some detail.  A sedimentary facies log is provided on p102 including detailed descriptions of its lithology and depositional environments. Coal and carbonaceous shale of this unit are the second most important source rocks in the Cooper Basin. Coal thickness exceeds 35m in the Patchawarra Trough and 25m in the Weena Trough. Reservoir characteristics discussed.  Unconformably overlies the Daralingie Formatio, Epsilon Formation and the Murteree Shale. Overlain conformably by the Arrabury Formation (Nappamerri Group). See also xii, p50, p58, p63-p67, p69 fig 6.1, p70-p73, p89, p93, p96, p99, p101-p105, p119, p122, p125, p127, p129, p131, p132 tbl 8.1-8.2, p133, p138 fig 8.17, p139 fig 8.18, p141, p144 fig 9.2, p146, p148-p153, p157, p159-p162, p164-p165, p168, p170-p171, p173-p176, p182-p183, p187, p191-p193, p195, p204-p205, p216.||Gidgealpa Group||Disconformably overlies the Patchawarra Formation.|Interbedded buff to white, fine to coarse-grained sandstone, dark grey siltstone and dark grey to black carbonaceous shale that is sometimes sideritic with thin coal seams and conglomerates.|
18357|Toolachee Formation|13516|6|Mentioned|p147, fig 5, p155|Late Permian|Late Permian|From Cooper Basin||||||
18357|Toolachee Formation|22527|6|Mentioned|p 1|||||||||
18357|Toolachee Formation|22817|5|Briefly described|p28|Late Permian|Late Permian|||||||
18357|Toolachee Formation|22839|6|Mentioned|P33||Late Permian|||||||
18357|Toolachee Formation|22883|6|Mentioned|P29|||Overlying unit is Arrabury Formation||||||
18357|Toolachee Formation|22909|5|Briefly described|42|||||||||
18357|Toolachee Formation|22924|6|Mentioned|49|||||||||
18357|Toolachee Formation|23154|5|Briefly described|Map Legend|Late Permian|Late Permian|Geological Province - Cooper Basin. Of the Gidgealpa Group.||||||12-DEC-06
18357|Toolachee Formation|23155|4|Described|p22|Late Permian|Late Permian|Age determined from palynological evidence.  The unit consitutes the top unit of the Gidgealpa Group.  Max thickness is about 152m in the Toolachee- Munkarie area.  On STRZELECKI the Toolachee Formation is overlain conformably by Arrabury Formation.||||||
18357|Toolachee Formation|23375|4|Described|Fig2 p265|Dzhulfian|Midian|In the Cooper Basin.||||||12-DEC-06
18357|Toolachee Formation|23832|4|Described|p330|Permian|Permian|Of Gidgealpa Group. Geological Province: Cooper Basin.||||||
18357|Toolachee Formation|24199|5|Briefly described|p512|Late Permian|Late Permian|Geological Province: Cooper Basin.||||||
18357|Toolachee Formation|24210|5|Briefly described|p133 Fig. 2|Late Permian|Late Permian|Of the Gidgealpa Group.  Geological Province: Cooper Basin.  See also p132.||||||
18357|Toolachee Formation|24212|6|Mentioned|p67, p69, p75|||Geological Province: Cooper Basin.||||||
18357|Toolachee Formation|24240|5|Briefly described|p21|Permian|Permian|Geological Province: Cooper Basin.||||||
18357|Toolachee Formation|29387|6|Mentioned|Table 2|||Refers to Gatehouse(1972).||||||
18357|Toolachee Formation|29389|6|Mentioned|p18|||Permian.||||||
18357|Toolachee Formation|29391|6|Mentioned|Table 5|||Appears on p23.||||||12-DEC-06
18357|Toolachee Formation|29513|6|Mentioned|p23|||||||||
18357|Toolachee Formation|29518|6|Mentioned|p24|||||||||
18357|Toolachee Formation|29520|6|Mentioned|p18|||||||||
18357|Toolachee Formation|29526|6|Mentioned|p18|||||||||
18357|Toolachee Formation|29721|6|Mentioned|p165|||||||||
18357|Toolachee Formation|29729|6|Mentioned|p266|||||||||
18357|Toolachee Formation|30515|6|Mentioned|p66|||See also p68. Part of Gidgealpa Group.||||||12-DEC-06
18357|Toolachee Formation|30519|5|Briefly described|p73|||Part of Gidgealpa Group. See also p75.||||||12-DEC-06
18357|Toolachee Formation|30540|6|Mentioned|p65|||General geology||||||
18357|Toolachee Formation|30543|6|Mentioned|p104|||||||||
18357|Toolachee Formation|30544|6|Mentioned|p53|||||||||
18357|Toolachee Formation|30825|6|Mentioned|p37|||||||||
18357|Toolachee Formation|30873|2|Defined|p13|Permian|Permian|Part of Gidgealpa Group.||||||12-DEC-06
18357|Toolachee Formation|30921|6|Mentioned|Map legend|Tatarian|Kungurian|Kungurian - Tatarian||||||
18357|Toolachee Formation|32696|6|Mentioned|Fig.4|||See also Figs. 6,7,8,9||||||
18357|Toolachee Formation|33074|6|Mentioned|p260|||||||||
18357|Toolachee Formation|33192|6|Mentioned|p18|||||||||
18357|Toolachee Formation|33331|6|Mentioned|p40|||||||||
18357|Toolachee Formation|33372|6|Mentioned|p25|||||||||
18357|Toolachee Formation|33489|3|Fully described|p42|||Structural and sedimentological development.||||||12-DEC-06
18357|Toolachee Formation|33976|6|Mentioned|Fig.5|||||||||
18357|Toolachee Formation|34839|6|Mentioned|Fig.2|||||||||
18357|Toolachee Formation|35067|6|Mentioned|Fig.4|||||||||
18357|Toolachee Formation|35068|6|Mentioned|Fig.3|||||||||
18357|Toolachee Formation|35151|6|Mentioned|p147|||||||||
18357|Toolachee Formation|35279|6|Mentioned|p19|||||||||
18357|Toolachee Formation|35457|6|Mentioned|p629|||Also Fig.4 biostratigraphic relationships||||||
18357|Toolachee Formation|35573|6|Mentioned|Fig.7|||Generalised stratigraphy - Southern Cooper Basin||||||
18357|Toolachee Formation|35845|4|Described|p24|||Lithology and depositional environments. See also Fig.25.||||||17-JAN-08
18357|Toolachee Formation|36099|6|Mentioned|p191|||||||||
18357|Toolachee Formation|36331|6|Mentioned|Fig.5|||||||||
18357|Toolachee Formation|36613|6|Mentioned|p1864|||||||||
18357|Toolachee Formation|36643|6|Mentioned|Table 1|||||||||
18357|Toolachee Formation|36910|6|Mentioned|p61|||||||||
18357|Toolachee Formation|36917|6|Mentioned|p143|||||||||
18357|Toolachee Formation|36924|6|Mentioned|Table 1|||||||||
18357|Toolachee Formation|37065|6|Mentioned|p32|||||||||
18357|Toolachee Formation|37103|5|Briefly described|p266|||||||||
18357|Toolachee Formation|37287|6|Mentioned|p36|||||||||
18357|Toolachee Formation|37565|6|Mentioned|Fig.8|||||||||
18357|Toolachee Formation|37703|6|Mentioned|p2240|||||||||
18357|Toolachee Formation|37855|6|Mentioned|p4|||||||||
18357|Toolachee Formation|37917|6|Mentioned|Fig.2|||||||||
18357|Toolachee Formation|38730|6|Mentioned|p29|||||||||
18357|Toolachee Formation|38908|6|Mentioned|p8|||||||||
18357|Toolachee Formation|38958|5|Briefly described|p495|||||||||
18357|Toolachee Formation|38977|6|Mentioned|Fig.1|||||||||
18357|Toolachee Formation|39252|5|Briefly described|p20|||See also p26, p28 and Fig.15.||||||12-DEC-06
18357|Toolachee Formation|39254|5|Briefly described|p46|||See also p47.||||||12-DEC-06
18357|Toolachee Formation|39255|6|Mentioned|p51|||||||||
18357|Toolachee Formation|39261|6|Mentioned|Fig. 9|||||||||
18357|Toolachee Formation|39264|6|Mentioned|Fig. 13|||||||||
18357|Toolachee Formation|39276|6|Mentioned|p335|||oil & gas in Tartulla No.1||||||
18357|Toolachee Formation|39445|5|Briefly described|Table 8|||||||||
18357|Toolachee Formation|39478|6|Mentioned|Table 1|||||||||
18357|Toolachee Formation|39494|6|Mentioned|Fig.3|||||||||
18357|Toolachee Formation|39757|6|Mentioned|p1601|||||||||
18357|Toolachee Formation|40030|6|Mentioned|Fig.3|||||||||
18357|Toolachee Formation|40056|1|Redefined|p11|Late Permian|Late Permian|||||||
18357|Toolachee Formation|40249|6|Mentioned|p45|||||||||
18357|Toolachee Formation|40544|6|Mentioned|p156|||||||||
18357|Toolachee Formation|40637|6|Mentioned|Fig.2|||||||||
18357|Toolachee Formation|41060|6|Mentioned|Fig.5|||||||||
18357|Toolachee Formation|41099|6|Mentioned|p185|||||||||
18357|Toolachee Formation|41123|6|Mentioned|p180|||||||||
18357|Toolachee Formation|41131|5|Briefly described|Table 1|||||||||
18357|Toolachee Formation|41164|6|Mentioned|p422|||||||||
18357|Toolachee Formation|41165|6|Mentioned|Fig.18|||||||||
18357|Toolachee Formation|41176|6|Mentioned|p206|||||||||
18357|Toolachee Formation|41183|6|Mentioned|Fig.3 p308|||||||||
18357|Toolachee Formation|41184|6|Mentioned|p348|||||||||
18357|Toolachee Formation|41189|6|Mentioned|p249|||||||||
18357|Toolachee Formation|41195|6|Mentioned|p325|||||||||
18357|Toolachee Formation|41198|6|Mentioned|p44|||||||||
18357|Toolachee Formation|41214|6|Mentioned|p256|||||||||
18357|Toolachee Formation|41223|6|Mentioned|p407|||||||||
18357|Toolachee Formation|41267|6|Mentioned|p256|||||||||
18357|Toolachee Formation|41288|6|Mentioned|p159|||||||||
18357|Toolachee Formation|41536|6|Mentioned|p373|||||||||
18357|Toolachee Formation|41595|6|Mentioned|p31|||||||||
18357|Toolachee Formation|41689|6|Mentioned|Table 1|||||||||
18357|Toolachee Formation|41707|6|Mentioned|Fig.8|||||||||
18357|Toolachee Formation|41712|6|Mentioned|p282|||See also P289||||||
18357|Toolachee Formation|42006|6|Mentioned|Fig.1 P21|||||||||
18357|Toolachee Formation|42008|6|Mentioned|p270|||||||||
18357|Toolachee Formation|42084|6|Mentioned|Fig.3 P356|||||||||
18357|Toolachee Formation|42085|6|Mentioned|Fig.2 P374|||||||||
18357|Toolachee Formation|42150|6|Mentioned|p65|||||||||
18357|Toolachee Formation|42187|6|Mentioned|Fig.2 P318|||||||||
18357|Toolachee Formation|42256|6|Mentioned|Fig.1 P243|||||||||
18357|Toolachee Formation|42395|6|Mentioned|p80|||||||||
18357|Toolachee Formation|42496|5|Briefly described|App.1 P152, Fig.3 P2|||||||||
18357|Toolachee Formation|42599|6|Mentioned|p624|||Cooper Basin.||||||
18357|Toolachee Formation|42648|5|Briefly described|p41, p48|||||||||
18357|Toolachee Formation|42746|5|Briefly described|p6|||||||||
18357|Toolachee Formation|42999|5|Briefly described|Table 2,p90||Late Permian|||||||
18357|Toolachee Formation|43002|5|Briefly described|Fig.2,p135|||||||||
18357|Toolachee Formation|43105|5|Briefly described|Fig.7,p13|||||||||
18357|Toolachee Formation|43570|6|Mentioned|Fig.2,p535|Late Permian|Early Permian|(Kayanian-Tatarian)||||||
18357|Toolachee Formation|43628|6|Mentioned|Fig.3|Late Permian|Late Permian|||||||
18357|Toolachee Formation|44133|4|Described|p65 Fig. 8.3, 82, 85|Tatarian|Kazanian|Of the Gidgealpa Group. Geological Province: Cooper Basin. Conformably overlain by the Arrabury Formation (Nappamerri Group). Maximum Thickness: 160m.||||||17-JAN-08
18357|Toolachee Formation|46849|6|Mentioned|p191|||||||||
18357|Toolachee Formation|48995|6|Mentioned|p50|||See also P50.||||||
18357|Toolachee Formation|60386|6|Mentioned|p296|Lopingian|Guadalupian|Cooper Basin. Non-marine. Age shown as Ufimian to Changhsingian.||||||
18357|Toolachee Formation|60717|5|Briefly described|p40|Middle Triassic|Late Permian|Of the Nappamerri Group. Overlain by Arrabury Formation. Thickness: 160m. Geological Province: Cooper Basin. See also Figure 2.||||||31-JAN-08
18357|Toolachee Formation|61613|6|Mentioned|p282 Fig. 2|Late Permian|Late Permian|Geological Province: Cooper and Simpson Basins.||||||07-FEB-11
18357|Toolachee Formation|61614|5|Briefly described|p289, p290, p290 Fig. 2|Late Permian|Late Permian|Of Gidgealpa Group. Geological Province: Cooper Basin. Contain coal and shale lithologies.||||||17-MAR-09
18357|Toolachee Formation|61615|5|Briefly described|p302, p303, p302 Fig. 2, p304, p307|Late Permian|Late Permian|Of Gidgealpa Group. Conformably overlain by Nappamerri Group. Geological Province: Cooper Basin. Deposited in a fluvial, peat swamps and lacustrine environments.||||||07-FEB-11
18357|Toolachee Formation|61616|6|Mentioned|p329|Permian|Permian|Of Gidgealpa Group. Geological Province: Cooper Basin.||||||
18357|Toolachee Formation|61617|6|Mentioned|p343, p346|Permian|Permian|Geological Province: Cooper Basin.||||||
18357|Toolachee Formation|62046|5|Briefly described|p125 Fig. 2|Permian|Permian|Geological Province: Cooper-Eromanga Basins.||||||14-APR-08
18357|Toolachee Formation|62537|6|Mentioned|p191 Fig.2. |Late Permian|Late Permian|Cooper Basin.||Unit in Gidgealpa Group.||Is overlain by Callamurra Member of the Arrabury Formation.||
18357|Toolachee Formation|62730|5|Briefly described|p352 Fig. 1|Late Permian|Late Permian|Geological Province: Cooper Basin.||||||21-APR-08
18357|Toolachee Formation|63832|6|Mentioned|p131 fig 2|Lopingian|Guadalupian|Of Cooper Basin.||||||
18357|Toolachee Formation|63978|2|Defined|p17, Fig. 3|Late Permian|Middle Permian|Originally included upper Gidgealpa Gp. Disconformable on Daralingie Fm; also unconformable on Patchawarra Fm.in places; conformable below Arrabury Fm. Max. thick:190m. Interbedded sandst., siltstone, mudstone + shale?.detailed lith. incl. In Cooper Basin||||||27-NOV-15
18357|Toolachee Formation|64048|5|Briefly described|p63, p64 Tb. 2, p66|Late Permian|Permian|Max. thickness: >150m. Source of hydrocarbons - coal measures. Hosts largest gas reservoir in SA. Geological Province: Cooper Basin.||||||07-FEB-11
18357|Toolachee Formation|64197|6|Mentioned|p625 Fig.1c, p630 Fig.7|Late Permian|Late Permian|Cooper Basin.||||Underlies the Callamurra Member of the Nappamerri Group.||11-DEC-15
18357|Toolachee Formation|64631|5|Briefly described|p44 Fig.2.|Changhsingian|Wordian|Cooper Basin. Biostratigraphic age control for base and top.||||Is overlain by Nappamerri Group. Unconformably underlain by Daralingi Formation.||
18357|Toolachee Formation|64665|5|Briefly described|p53 Fig.2, p56.|Late Permian|Middle Permian|Cooper Basin. Hosts coal: equivalent to Betts Creek beds (Galilee Basin) and Bandanna Formation (Bowen Basin). Inertinite-rich, vitrinite-poor; medium volatile bituminous to anthracite. Located at uneconomic depths; source rock maturation has produced substantial oil and gas production.||||Is overlain by Arrabury Formation.||
18357|Toolachee Formation|65238|5|Briefly described|p9|Late Permian|Late Permian|Geological province: Cooper Basin. In sedimentary continuum with the overlying Arrabury Formation.||||||17-FEB-10
18357|Toolachee Formation|65489|5|Briefly described|p15, p45, p47-50, p73, p96, p131-132|Permian|Permian|Cooper Basin. 160m thick. Gas and oil reservoir accounting for 56% and 0.6% respectively of the Basin's production. Regarded as the richest source unit in the Cooper-Eromanga Basins. Mis-spelt as Toollachee on p48.||Unit in Gidgealpa Group.||Unconformably overlies Daralingie Formation. Is overlain conformably by Arrabury Formation (Nappamerri Group).|Includes multi-zone high-sinuosity fluvial sandstones.|
18357|Toolachee Formation|65925|5|Briefly described|Appendix 2.||||||||Sandstone; mudstone; coal. Mixed-load channels, flood-plain and swamp.|
18357|Toolachee Formation|67402|5|Briefly described|p43 tbl HPB1, p90-p94|||Cooper Basin. Highly prospective reservoir formation for the storage of carbon dioxide with a potential storage capacity of 43.2 Megatonnes. Deposited in a meandering fluvial environment. See also p96, p98, p99 fig CPR14, p100, p101, p101 tbl CPR2, p103-p105, p268, p303.||Gidgealpa Group||Unconformably overlies the Daralingie Formation. Conformably overlain by the Callamurra Member.|Fining upwards deposits of coarse-grained sandstone, coal, carbonaceous siltstone, mudstone and shale.|
18357|Toolachee Formation|68731|5|Briefly described|p200 Fig 3.110, p204, p206, p207|Lopingian|Guadalupian|Cooper Basin. Originally incorporated rocks now assigned to the Daralingie Formation. Detailed lithology discussed. ~ < 190 m thick. Contains late Capitanian(?)-Lopingian palynofloras. Disconformably underlain by the Daralingie Formation.||Of the Gidgealpa Group.|Includes the Munkarie beds (basal unit).|Unconformably underlain by the Patchawarra and Epsilon Formations, and the Murteree and Roseneath Shales. Conformably overlain by the Arrabury Formation and the Callamurra Member.|Includes interbedded sandstone, siltstone, mudstone and shale, commonly in upwardly fining packages in the lower part.|12-MAY-16
18357|Toolachee Formation|69023|5|Briefly described|p81-82, p150-151|Permian|Permian|Cooper Basin. Oil and gas reserves.||Unit in Gidgealpa Group.||Disconformably overlies Daralingie Formation. Unconformably overlies Gidgealpa Group. Is overlain by Nappamerri Group.|Basal conglomerates with exotic clasts sourced from uplifted Warburton Basin.|
18357|Toolachee Formation|69454|5|Briefly described|p38:4|Changhsingian|Capitanian|Cooper Basin.||Gidgealpa Group.||||12-JUL-16
18357|Toolachee Formation|69594|5|Briefly described|p524|||Cooper Basin.||||Is overlain unconformably by Poolowanna Formation.||
18357|Toolachee Formation|69673|6|Mentioned|p153 fig 125|||||Gidgealpa Group||Overlain by Arrabury Formation, overlies Daralingie Formation||
18357|Toolachee Formation|69728|6|Mentioned|p285|||Cooper Basin.||Gidgealpa Group.||||
18357|Toolachee Formation|69797|5|Briefly described|p17 Fig.2|Late Permian|Late Permian|Age: Kazanian - Tatarian (approximated from figure). Geol. Prov: Cooper Basin.||Gidgealpa Group||||
18357|Toolachee Formation|69946|5|Briefly described|p9, p36, p54|Permian|Permian|Cooper Basin. Kazanian-Tatarian.||Uppermost unit in Gidgealpa Group.||Unconformably overlies Daralingie Formation. Is overlain conformably by Arrabury Formation (Nappamerri Group).||
18357|Toolachee Formation|69947|5|Briefly described|p13 Fig.7.2|Permian|Permian|Cooper Basin.||Gidgealpa Group.||||
18357|Toolachee Formation|69982|5|Briefly described|p14|||||||Unconformably overlies Mooracoochie Volcanics and Dullingari Group.|Includes basal conglomerate.|
18357|Toolachee Formation|70317|6|Mentioned|p33, 36|Late Permian|Late Permian|Cooper Basin. Vertical section showing fracture densities.||Gidgealpa Group.||Unconformably overlies Daralingie Formation (Gidgealpa Group). Is overlain by Callamurra Member (Arrabury Formation).||
18357|Toolachee Formation|70823|4|Described|iv, p1-p3, p6, p14|Changhsingian|Wuchiapingian|Cooper Basin. Hosts deep, dry coal seam gas. Seismic reflection, outcrop and palynological characteristics and coal thicknesses discussed. Up to 280m thick. Deposited in a meandering fluvial to deltaic environment. Hosts a commercial reservoir. Conformably overlain by the Callamurra Member of the Arrabury Formation. See also p25-p27, p39-p41, p53-p54, p58-p59, p61, p66, p70-p75, p78-p81, p83.||Gidgealpa Group||Disconformably overlies the Daralingie Formation. Unconformably overlies the Patchawarra Formation, Epsilon Formation and the Murteree Shale.|Interbedded fine to coarse-grained quartzose sandstone, mudstone, carbonaceous shale with thin coal seams and conglomerates.|
18357|Toolachee Formation|70824|4|Described|p1-p3, p5, p8-p9, p19, p28|Changhsingian|Wuchiapingian|Cooper Basin. Together with the Patchawarra Formation these are the richest, thickest and most extensive source rocks. Hosts deep dry coal seam gas. Up to 280m thick. Deposited in meandering fluvial to slightly deltaic environments. Outcrop and areal extent are discussed briefly in addition to source rock geochemistry. See also p30-p31, p66, p77, p84, p93-p95-p97, p99-p103, p108-p110, p113, p123.||||Unconformably overlies the Daralingie Formation. Overlain by the Callamurra Member (Arrabury Formation).|Interbedded fine to coarse-grained quartzose sandstone, mudstone, carbonaceous shale with thin coal seams and conglomerates.|
18357|Toolachee Formation|70946|5|Briefly described|p1087, p1089-1090|Permian|Permian|Cooper Basin. Hosts shallow and deep dry coal seam gas accumulations. Deposited in a meandering fluvial, partly deltaic environment.||Gidgealpa Group.||Unconformably overlies Daralingie Formation. Overlain by the Arrabury Formation.||08-OCT-18
18357|Toolachee Formation|71265|5|Briefly described|p589|Changhsingian|Wuchiapingian|Cooper Basin.||Gidgealpa Group.||Unconformably overlies Daralingie Formation. Is overlain unconformably by Arrabury Formation.||
18357|Toolachee Formation|71342|5|Briefly described|Ch5 p9, Ch5 p36, Ch5 p54|Tatarian|Kazanian|Cooper Basin. Palynological zone is given in fig 5.3 Ch5 p36. Deposited in a meandering fluvial or deltaic environment. See also Ch7 p13, Ch10 tbl 10.1, Ch10 p7, Ch10 p17-p20.||Gidgealpa Group||Unconformably overlies the Daralingie and Epsilon Formations. Conformably overlain by the Arrabury Formation.||
18357|Toolachee Formation|71701|5|Briefly described|p155|Changhsingian|Wuchiapingian|Cooper Basin.||Gidgealpa Group||Unconformably overlies the Daralingie Formation. Overlain by the Arrabury Formation.||09-FEB-23
18357|Toolachee Formation|72297|5|Briefly described|p697, p739, p742-743|Permian|Permian|Cooper Basin. Contains coal, but at too great a depth for economic extraction. One of the main petroleum source rocks within the Basin; also a reservoir. Also contains significant gas.||||||
18357|Toolachee Formation|73167|5|Briefly described|p662, p664, p666|late Permian|late Permian|Cooper Basin. Contains oil and gas, hydrocarbon source.||||Unconformably overlies the Daralingie Formation, underlies the Nappamerri Group.|Meandering fluvial to deltaic sediments.|
18357|Toolachee Formation|73244|6|Mentioned|p86|Permian|Permian|Cooper Basin. Meandering fluvial, deltaic environment. Oil, gas, and source rock.||||||
18357|Toolachee Formation|73251|6|Mentioned|p62|Lopingian|Guadalupian|Cooper Basin. Meandering fluvial depositional environment; deltaic in part. Hydrocarbon source rock that contains[?] gas and oil. Overlies the Daralingie Unconformity.||Gidgealpa Group||Overlain by Arrabury Formation including Callamurra Member.||
18357|Toolachee Formation|73343|5|Briefly described|p337-338|Late Permian|Late Permian|Cooper Basin. Source rock that hosts oil and gas. Reflect meandering fluvial to deltaic settings.||||Unconformably underlain by Daralingie Formation and Roseneath Shale. Overlain by Nappamerri Group including Callamurra Member.||
18357|Toolachee Formation|73479|5|Briefly described|p156 Fig.2, p159, p161, p163-166|Permian|Permian|Cooper Basin. Meandering fluvial to deltaic depositional environment. Most organic-rich source rock in basin. Associated with Daralingie Event.|ca 250 Ma|||Unconformably overlies Daralingie Formation, Roseneath Shale, underlies Nappamerri Group, Callamurra Member|Sands, shales and coals.|
18357|Toolachee Formation|73495|6|Mentioned|p499|Changhsingian|Wuchiapingian|||||||
18365|Toolbrenup beds|30144|5|Briefly described|p82|||||||||
18375|Toolebuc Formation|12597|5|Briefly described|p492 Tb.1, p500|Albian|Albian|Eromanga Basin. 3-75m thick. Characteristic high gamma response. Contains abundant bivalves, fish skeletons and teeth, radiolarians, globigerinids and dinoflagellates.|||||Carbonaceous and calcareous mudstone and limestone with minor thin interbeds of fine-grained calcareous labile sandstone and siltstone; local 10m thick oil-shale horizon in N.|
18375|Toolebuc Formation|13497|5|Briefly described|p115, p115 fig 6.33, p146|Early Cretaceous|Early Cretaceous|Eromanga Basin.||Marree Subgroup||Overlies the Wallumbilla Formation. Overlain by the Allaru Mudstone.|Shale and siltstone with minor shoreface sandstone.|
18375|Toolebuc Formation|13516|6|Mentioned|p167 fig 10, p169 fig 11, p171 fig 12|Albian|Albian|In Eromanga Basin.||||||
18375|Toolebuc Formation|22464|5|Briefly described|p9||Early Cretaceous|In the Eromanga Basin. Overlies Wallumbilla Formation.||||||12-DEC-06
18375|Toolebuc Formation|22857|5|Briefly described|p295, p296-7 Tb.22.1, p314|Albian|Albian|Oil shales occur. Together with Allaru Mudstone thickness is ~100m. Geological Province: Eromanga Basin||||||
18375|Toolebuc Formation|22865|4|Described|p295,Table22.1p296-7|Cenomanian|Albian|||||||
18375|Toolebuc Formation|22883|5|Briefly described|Fig2 P30||Early Cretaceous|Overlain by Allaru Mudstone, underlain by Wallumbilla Formation.||||||01-FEB-07
18375|Toolebuc Formation|22912|5|Briefly described|33|||Geological province: Eromanga Basin.||||||12-DEC-06
18375|Toolebuc Formation|23031|5|Briefly described|31|||||||||
18375|Toolebuc Formation|23056|6|Mentioned|12 table 2|||||||||
18375|Toolebuc Formation|23154|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|Geological Province - Eromanga Basin.  Of the Marree Subgroup (Neales River Group) - not clear in legend however.||||||14-DEC-06
18375|Toolebuc Formation|23155|4|Described|p32|Early Cretaceous|Early Cretaceous|The formation is restricted to the northern and western STRZELECKI.||||||
18375|Toolebuc Formation|23356|5|Briefly described|26 Tab.2|Albian|Albian|||||||
18375|Toolebuc Formation|23375|4|Described|Fig2 p265, 266||Albian|Laterally equivalent to lower Oodnadatta Formation. In the Eromanga Basin.||||||12-DEC-06
18375|Toolebuc Formation|23393|5|Briefly described|p24|Early Cretaceous|Early Cretaceous|Of Rolling Downs Group.||||||
18375|Toolebuc Formation|23425|4|Described|Table 9.7 p394||Albian|see also p378. Of Rolling Downs Group. Overlain by Allaru Mudstone; underlain by Wallumbilla Formation. Carpentaria Basin Province.||||||12-DEC-06
18375|Toolebuc Formation|23430|4|Described|p522 + p524 Table 14.7|||In the Eromanga Basin Province.||||||12-DEC-06
18375|Toolebuc Formation|23431|5|Briefly described|p543|||||||||
18375|Toolebuc Formation|23518|5|Briefly described|p13|Mesozoic|Mesozoic|Of Rolling Downs Group.  Geological Province: Carpentaria Basin.||||||
18375|Toolebuc Formation|23864|6|Mentioned|p128|Albian|Albian|||||||
18375|Toolebuc Formation|23883|5|Briefly described|p129 Fig. 11.2|Cretaceous|Cretaceous|Of Rolling Downs Group.  Geological Province: Great Australian Superbasin.||||||
18375|Toolebuc Formation|23911|5|Briefly described|p97 Fig. 11|Cretaceous|Cretaceous|Geological Province: Eromanga Basin.  Of the Rolling Downs Group.||||||
18375|Toolebuc Formation|23982|5|Briefly described|p12|Cretaceous|Cretaceous|Of the Rolling Downs Group. Geological Province: Eromanga Basin. See also page 35 Fig.7.||||||
18375|Toolebuc Formation|23986|5|Briefly described|p71|||||||||
18375|Toolebuc Formation|24048|5|Briefly described|p76|||||||||
18375|Toolebuc Formation|24085|5|Briefly described|p33, p36, p38|Albian|Albian|Geological Province: Eromanga Basin.||||||16-SEP-08
18375|Toolebuc Formation|24092|5|Briefly described|p8 Fig.3|||Of Rolling Downs Group. Geological Province: Eromanga Basin.||||||
18375|Toolebuc Formation|24175|5|Briefly described|p17 Fig. 3|Albian|Albian|Geological Province: Eromanga Basin.||||||
18375|Toolebuc Formation|24201|5|Briefly described|p379|Albian|Albian|Geological Province: Eromanga Basin.||||||
18375|Toolebuc Formation|24204|5|Briefly described|p263 Fig.4, p267, p282 Fig.21|Early Cretaceous|Early Cretaceous|Geological Province: Eromanga Basin.||||||17-DEC-04
18375|Toolebuc Formation|24210|5|Briefly described|p133 Fig. 2|Early Cretaceous|Early Cretaceous|Of the Marree Subgroup.  Geological Province: Eromanga Basin.||||||
18375|Toolebuc Formation|24226|5|Briefly described|p391|Albian|Albian|Age: Late Albian.||||||
18375|Toolebuc Formation|24243|5|Briefly described|p3 Fig.2|Cretaceous|Cretaceous|Of Rolling Downs Group.||||||
18375|Toolebuc Formation|24251|5|Briefly described|p234 Fig.1, p245|Albian|Albian|Overlying Unit: Allaru Formation. Underlying Unit: Wallumbilla Formation. Maximum Thickness: <35m. Geological Province: Eromanga Basin||||||
18375|Toolebuc Formation|29394|6|Mentioned|p145|||Cretaceous.||||||
18375|Toolebuc Formation|30584|4|Described|Table 1|||||||||
18375|Toolebuc Formation|30585|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
18375|Toolebuc Formation|31121|6|Mentioned|Table 2|||||||||
18375|Toolebuc Formation|31165|6|Mentioned|Table 1|||||||||
18375|Toolebuc Formation|31168|6|Mentioned|p10|||||||||
18375|Toolebuc Formation|32314|6|Mentioned|Fig. 4|||||||||
18375|Toolebuc Formation|32705|6|Mentioned|p188|||||||||
18375|Toolebuc Formation|33017|6|Mentioned|p1|||See also p8.||||||12-DEC-06
18375|Toolebuc Formation|33075|4|Described|p451|||Type section p455.||||||12-DEC-06
18375|Toolebuc Formation|33078|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
18375|Toolebuc Formation|33079|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
18375|Toolebuc Formation|33086|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower to Upper Cretaceous||||||
18375|Toolebuc Formation|33176|6|Mentioned|p175|||||||||
18375|Toolebuc Formation|33177|6|Mentioned|p12|||||||||
18375|Toolebuc Formation|33178|6|Mentioned|p11|||||||||
18375|Toolebuc Formation|33179|4|Described|p11|||||||||
18375|Toolebuc Formation|33368|6|Mentioned|p27|||Refers Smart (1972).||||||
18375|Toolebuc Formation|33414|6|Mentioned|p212,213,Tb.|||Part of Wilgunya Sub-group.||||||
18375|Toolebuc Formation|33772|6|Mentioned|p13|||||||||
18375|Toolebuc Formation|33773|6|Mentioned|p17|||||||||
18375|Toolebuc Formation|33900|6|Mentioned|p21|||||||||
18375|Toolebuc Formation|34811|4|Described|Table 1|||||||||
18375|Toolebuc Formation|35220|6|Mentioned|Table 2|||||||||
18375|Toolebuc Formation|35239|6|Mentioned|p258|||||||||
18375|Toolebuc Formation|35253|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
18375|Toolebuc Formation|35457|6|Mentioned|p623|||||||||
18375|Toolebuc Formation|35560|4|Described|p291|||||||||
18375|Toolebuc Formation|35640|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
18375|Toolebuc Formation|35663|6|Mentioned|Fig.2|||Subsurface correlations of the central basin rock units.||||||
18375|Toolebuc Formation|35793|6|Mentioned|Fig.3|||||||||
18375|Toolebuc Formation|35811|5|Briefly described|Table 3|||Uranium exploration discussed p556.||||||12-DEC-06
18375|Toolebuc Formation|35855|6|Mentioned|Fig.2|||Early Cretaceous lithostratigraphy.||||||
18375|Toolebuc Formation|35936|6|Mentioned|p615|||||||||
18375|Toolebuc Formation|36012|3|Fully described|Table 5|||See also p18.||||||12-DEC-06
18375|Toolebuc Formation|36110|6|Mentioned|p47|||||||||
18375|Toolebuc Formation|36228|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
18375|Toolebuc Formation|36229|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
18375|Toolebuc Formation|36243|6|Mentioned|Table 6A|||||||||
18375|Toolebuc Formation|36251|4|Described|p3|||||||||
18375|Toolebuc Formation|36331|6|Mentioned|p92|||||||||
18375|Toolebuc Formation|36552|6|Mentioned|p61|||||||||
18375|Toolebuc Formation|36571|6|Mentioned|p95|||||||||
18375|Toolebuc Formation|36690|6|Mentioned|p47|||||||||
18375|Toolebuc Formation|36713|5|Briefly described|p361|||||||||
18375|Toolebuc Formation|36910|6|Mentioned|p61|||||||||
18375|Toolebuc Formation|36912|6|Mentioned|Fig.3|||||||||
18375|Toolebuc Formation|36922|6|Mentioned|Fig.3|||||||||
18375|Toolebuc Formation|37287|6|Mentioned|p36|||||||||
18375|Toolebuc Formation|37608|3|Fully described|Table 1|||||||||
18375|Toolebuc Formation|37776|6|Mentioned|Fig.2|||||||||
18375|Toolebuc Formation|38011|6|Mentioned|p126|||||||||
18375|Toolebuc Formation|38199|5|Briefly described|p426|||Palynology||||||
18375|Toolebuc Formation|38218|4|Described|p285|||||||||
18375|Toolebuc Formation|38226|6|Mentioned|Table 1|||||||||
18375|Toolebuc Formation|38325|4|Described|p265|||||||||
18375|Toolebuc Formation|38372|6|Mentioned|p647|||||||||
18375|Toolebuc Formation|38373|6|Mentioned|p618|||||||||
18375|Toolebuc Formation|38608|6|Mentioned|Map legend|Mesozoic|Mesozoic|||||||
18375|Toolebuc Formation|38779|6|Mentioned|p7|||||||||
18375|Toolebuc Formation|38780|6|Mentioned|p17|||||||||
18375|Toolebuc Formation|38814|6|Mentioned|Table 1|||||||||
18375|Toolebuc Formation|39029|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Overlain by Allaru Mudstone.||||||25-AUG-04
18375|Toolebuc Formation|39070|4|Described|p365|||||||||
18375|Toolebuc Formation|39211|5|Briefly described|Fig.3|||See also Figs 4,7,9,12-16 etc. Correlation.||||||12-DEC-06
18375|Toolebuc Formation|39445|5|Briefly described|Table 11|||||||||
18375|Toolebuc Formation|39478|6|Mentioned|Table 1|||||||||
18375|Toolebuc Formation|39480|6|Mentioned|p188|||||||||
18375|Toolebuc Formation|39481|6|Mentioned|p180|||||||||
18375|Toolebuc Formation|39482|6|Mentioned|Fig.7|||||||||
18375|Toolebuc Formation|39556|5|Briefly described|Map legend|Cretaceous|Cretaceous|||||||
18375|Toolebuc Formation|39575|6|Mentioned|p103|||||||||
18375|Toolebuc Formation|39708|4|Described|p477|||||||||
18375|Toolebuc Formation|39754|6|Mentioned|p1690|||||||||
18375|Toolebuc Formation|39797|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
18375|Toolebuc Formation|39799|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
18375|Toolebuc Formation|39846|6|Mentioned|Fig.2|||||||||
18375|Toolebuc Formation|39847|5|Briefly described|p39|||||||||
18375|Toolebuc Formation|39899|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
18375|Toolebuc Formation|39914|6|Mentioned|p3|||||||||
18375|Toolebuc Formation|39942|6|Mentioned|p463|||||||||
18375|Toolebuc Formation|39943|6|Mentioned|Table 8A|||||||||
18375|Toolebuc Formation|39989|6|Mentioned|p426|||||||||
18375|Toolebuc Formation|40121|6|Mentioned|Table 1|||||||||
18375|Toolebuc Formation|40167|6|Mentioned|p156|||||||||
18375|Toolebuc Formation|40199|6|Mentioned|Fig.1|||||||||
18375|Toolebuc Formation|40249|6|Mentioned|p41|||||||||
18375|Toolebuc Formation|40322|6|Mentioned|Fig.3|||||||||
18375|Toolebuc Formation|40452|6|Mentioned|p2|||||||||
18375|Toolebuc Formation|40648|6|Mentioned|p12|||||||||
18375|Toolebuc Formation|40670|6|Mentioned|Fig.9|||||||||
18375|Toolebuc Formation|40675|6|Mentioned|Table 8A|||||||||
18375|Toolebuc Formation|40687|6|Mentioned|Table 3|||||||||
18375|Toolebuc Formation|40719|5|Briefly described|p61|||||||||
18375|Toolebuc Formation|40771|5|Briefly described|p429|||||||||
18375|Toolebuc Formation|40801|6|Mentioned|p46|||||||||
18375|Toolebuc Formation|40926|6|Mentioned|p18|||||||||
18375|Toolebuc Formation|41012|3|Fully described|p137|||||||||
18375|Toolebuc Formation|41036|6|Mentioned|p220|||||||||
18375|Toolebuc Formation|41052|6|Mentioned|p87|||||||||
18375|Toolebuc Formation|41060|6|Mentioned|p2|||Generalized stratigraphy||||||
18375|Toolebuc Formation|41061|6|Mentioned|p19|||Generalized stratigraphy||||||
18375|Toolebuc Formation|41062|6|Mentioned|Fig.5|||||||||
18375|Toolebuc Formation|41063|6|Mentioned|p40|||||||||
18375|Toolebuc Formation|41064|6|Mentioned|p62|||||||||
18375|Toolebuc Formation|41084|5|Briefly described|Fig.2|||||||||
18375|Toolebuc Formation|41086|3|Fully described|p101|||See also Fig.3||||||
18375|Toolebuc Formation|41087|3|Fully described|p121|||||||||
18375|Toolebuc Formation|41088|4|Described|p141|||||||||
18375|Toolebuc Formation|41089|6|Mentioned|p156|||||||||
18375|Toolebuc Formation|41097|6|Mentioned|p166|||||||||
18375|Toolebuc Formation|41117|4|Described|p434|||||||||
18375|Toolebuc Formation|41121|6|Mentioned|p179|||||||||
18375|Toolebuc Formation|41125|6|Mentioned|p12|||||||||
18375|Toolebuc Formation|41165|5|Briefly described|p362, p368|||Mention Fig.20||||||
18375|Toolebuc Formation|41174|4|Described|p117|||||||||
18375|Toolebuc Formation|41175|6|Mentioned|Fig.1|||||||||
18375|Toolebuc Formation|41176|6|Mentioned|p206|||See also Table 2||||||
18375|Toolebuc Formation|41177|6|Mentioned|Fig.2|||||||||
18375|Toolebuc Formation|41178|6|Mentioned|p241|||||||||
18375|Toolebuc Formation|41179|6|Mentioned|p255|||||||||
18375|Toolebuc Formation|41180|5|Briefly described|p267|||||||||
18375|Toolebuc Formation|41181|6|Mentioned|p273|||||||||
18375|Toolebuc Formation|41182|5|Briefly described|p300|||||||||
18375|Toolebuc Formation|41183|6|Mentioned|p310|||||||||
18375|Toolebuc Formation|41184|6|Mentioned|p328|||||||||
18375|Toolebuc Formation|41187|6|Mentioned|Fig.2|||||||||
18375|Toolebuc Formation|41196|6|Mentioned|Fig.1|||||||||
18375|Toolebuc Formation|41198|6|Mentioned|Table 1|||||||||
18375|Toolebuc Formation|41214|6|Mentioned|Fig.3|||||||||
18375|Toolebuc Formation|41216|6|Mentioned|Fig.18|||||||||
18375|Toolebuc Formation|41219|6|Mentioned|p338|||||||||
18375|Toolebuc Formation|41266|6|Mentioned|Fig.3|||||||||
18375|Toolebuc Formation|41306|6|Mentioned|p4|||||||||
18375|Toolebuc Formation|41307|6|Mentioned|p5|||||||||
18375|Toolebuc Formation|41464|6|Mentioned|Map legend|Early Cretaceous||||||||
18375|Toolebuc Formation|41482|6|Mentioned|p37|||||||||
18375|Toolebuc Formation|41483|6|Mentioned|p49|||||||||
18375|Toolebuc Formation|41523|3|Fully described|p279|||||||||
18375|Toolebuc Formation|41556|6|Mentioned|Map legend|Early Cretaceous||||||||
18375|Toolebuc Formation|41568|5|Briefly described|p15|||||||||
18375|Toolebuc Formation|41707|6|Mentioned|p164|||||||||
18375|Toolebuc Formation|41724|6|Mentioned|p383|||||||||
18375|Toolebuc Formation|42061|4|Described|p155|||||||||
18375|Toolebuc Formation|42067|4|Described|Appendix 2|||||||||
18375|Toolebuc Formation|42071|6|Mentioned|p117|||||||||
18375|Toolebuc Formation|42084|6|Mentioned|Fig.3 P356|||||||||
18375|Toolebuc Formation|42085|6|Mentioned|Fig.2 P374|||||||||
18375|Toolebuc Formation|42374|6|Mentioned|p435|Albian||||||||
18375|Toolebuc Formation|42397|6|Mentioned|Fig.2 P3|||||||||
18375|Toolebuc Formation|42402|5|Briefly described|p115, 116|||||||||
18375|Toolebuc Formation|42429|6|Mentioned|p156|||||||||
18375|Toolebuc Formation|42446|4|Described|p13|||||||||
18375|Toolebuc Formation|42447|6|Mentioned|Fig.1|||||||||
18375|Toolebuc Formation|42496|5|Briefly described|p136, Fig.3 p132|||||||||
18375|Toolebuc Formation|42520|5|Briefly described|p6|||||||||
18375|Toolebuc Formation|42538|5|Briefly described|Fig. 25.2 P325|||||||||
18375|Toolebuc Formation|42585|5|Briefly described|p79|||||||||
18375|Toolebuc Formation|42588|5|Briefly described|p115|||||||||
18375|Toolebuc Formation|42637|4|Described|p11|||||||||
18375|Toolebuc Formation|42673|5|Briefly described|Fig.2, P184|||||||||
18375|Toolebuc Formation|42746|6|Mentioned|Fig.6 P8|||||||||
18375|Toolebuc Formation|42749|6|Mentioned|Fig.2 P27|||||||||
18375|Toolebuc Formation|42804|5|Briefly described|p115|||||||||
18375|Toolebuc Formation|42999|5|Briefly described|Table 2,p90||Early Cretaceous|||||||
18375|Toolebuc Formation|43002|5|Briefly described|Fig.2,p135|||||||||
18375|Toolebuc Formation|43004|5|Briefly described|Table 1,p179|||||||||
18375|Toolebuc Formation|43105|6|Mentioned|p15|||||||||
18375|Toolebuc Formation|43114|5|Briefly described|p15|||||||||
18375|Toolebuc Formation|43122|5|Briefly described|p29|||see also Fig. 2.||||||
18375|Toolebuc Formation|43591|6|Mentioned|p40|||||||||
18375|Toolebuc Formation|43602|6|Mentioned|191|||In Eromanga Basin. Of the Rolling Downs Group.||||||12-DEC-06
18375|Toolebuc Formation|43630|6|Mentioned|p70|||also Fig.4||||||
18375|Toolebuc Formation|44112|6|Mentioned|p82|||||||||
18375|Toolebuc Formation|44133|5|Briefly described|p122, 104 Fig. 9.11|Late Albian|Middle Albian|Geological Province: Eromanga Basin.||||||
18375|Toolebuc Formation|44291|14|Not recorded|p14|||||||||
18375|Toolebuc Formation|45145|3|Fully described|Table 5|||||||||
18375|Toolebuc Formation|45161|6|Mentioned|p67|||||||||
18375|Toolebuc Formation|46791|4|Described|p47|||||||||
18375|Toolebuc Formation|46872|6|Mentioned|p105|||||||||
18375|Toolebuc Formation|46937|5|Briefly described|Fig.10|||See also Table 1.||||||
18375|Toolebuc Formation|47042|4|Described|p171|||||||||
18375|Toolebuc Formation|47083|5|Briefly described|p20||Mesozoic|Of Rolling Downs Group.||||||
18375|Toolebuc Formation|48770|6|Mentioned|Fig.1|||||||||
18375|Toolebuc Formation|49010|6|Mentioned|Fig.4|||In the Eromanga Basin.||||||12-DEC-06
18375|Toolebuc Formation|49011|6|Mentioned|Fig.3|||In the Eromanga Basin.||||||12-DEC-06
18375|Toolebuc Formation|49254|14|Not recorded|?|||||||||
18375|Toolebuc Formation|49273|14|Not recorded|?|||||||||
18375|Toolebuc Formation|49278|14|Not recorded|?|||||||||
18375|Toolebuc Formation|49330|14|Not recorded|?|||||||||
18375|Toolebuc Formation|49338|14|Not recorded|?|||||||||
18375|Toolebuc Formation|50100|5|Briefly described|p23|Cretaceous|Cretaceous|Of the Rolling Downs Group.  Contains calcareous bituminous shale (oil shale).  Geological Province: Carpentaria and Eromanga Basins.||||||
18375|Toolebuc Formation|50332|5|Briefly described|p22, p93, p96|Mesozoic|Mesozoic|Geological Province: Carpentaria Basin. Main lithologies are mudstone, calcareous shale, limestone, sandstone and siltstone. Also contains calcareous bituminous shale (oil shale).||||||07-FEB-11
18375|Toolebuc Formation|60331|5|Briefly described|p34 Fig.3|Albian|Albian|Overlies Wallumbilla Formation. Overlain by Allaru Mudstone. Geological Province: Eromanga Basin.||||||
18375|Toolebuc Formation|60359|5|Briefly described|Map Legend|Mesozoic|Mesozoic|Limestone, calcareous sandstone.||||||
18375|Toolebuc Formation|60717|5|Briefly described|p40 Fig. 2|Early Cretaceous|Early Cretaceous|Overlies Wallumbilla Formation. Overlain by Allaru Mudstone. Lateral to Oodnadatta Formation. Geological Province: Eromanga  Basin.||||||31-JAN-08
18375|Toolebuc Formation|61312|5|Briefly described|p66, p73|Albian|Aptian|Of the Rolling Downs Group. In Queensland it consists of carbonaceous and bitumous shale and siltstone with limestone lenses. In Queensland, overlies Wallumbilla Formation and is overlain by Allaru Mudstone. Geological Province: Eromanga Basin.||||||16-JUN-06
18375|Toolebuc Formation|61544|5|Briefly described|p374.|Albian|Albian|Eromanga Basin. Contains marine oil shales which are geochemically similar to asphaltite strandings along the Bight coast.|||||Includes marine oil shales.|
18375|Toolebuc Formation|61611|6|Mentioned|p265 Fig. 3|Early Cretaceous|Early Cretaceous|Geological Province: Eromanga Basin.||||||13-MAR-09
18375|Toolebuc Formation|61613|6|Mentioned|p282 Fig. 2|Early Cretaceous|Early Cretaceous|Of Maree Subgroup. Geological Province: Eromanga Basin.||||||07-FEB-11
18375|Toolebuc Formation|61614|6|Mentioned|p290 Fig. 2|Early Cretaceous|Early Cretaceous|Geological Province: Eromanga Basin.||||||17-MAR-09
18375|Toolebuc Formation|62376|5|Briefly described|p84|Early Cretaceous|Early Cretaceous|Geological Province: Pedirka Basin.||||||09-FEB-10
18375|Toolebuc Formation|62537|6|Mentioned|p191 Fig.2. |Early Cretaceous|Early Cretaceous|Eromanga Basin.||||Overlies Bulldog Shale. Is overlain by Allaru Formation.||
18375|Toolebuc Formation|62730|5|Briefly described|p352 Fig. 1|Cretaceous|Cretaceous|Geological Province: Eromanga Basin.||||||21-APR-08
18375|Toolebuc Formation|62837|5|Briefly described|Stratigraphic columns|Early Cretaceous|Early Cretaceous|Of the Rolling Downs Group. Age: ~101-~98Ma. Geological Province: Southern Cape York and Burketown Depression.||||||01-MAR-10
18375|Toolebuc Formation|63979|2|Defined|p50, Fig. 44|Albian|Albian|Previously Toolebuc Member (Wilgunya Fm). Conformable over Wallumbilla Fm; overlain by Allaru Mudstone. Max.thick: 65m. Predominantly mudstone with thin layers of siltstone, sandstone and conglomerate, towards top; also contains limestone (incl. coquinite)||||||09-APR-13
18375|Toolebuc Formation|64048|5|Briefly described|p64 Tb. 2|||Source of hydrocarbons - oil shale. Geological Province: Eromanga Basin.||||||07-FEB-11
18375|Toolebuc Formation|64197|6|Mentioned|p625 Fig.1c, p630 Figs.6,7|Cretaceous|Cretaceous|Eromanga Basin.||Unit in Marree Subgroup.||Underlies Allaru Mudstone; overlies Wallumbilla Formation.||11-DEC-15
18375|Toolebuc Formation|64665|6|Mentioned|p62.|Cretaceous|Cretaceous|Eromanga Basin.||||||
18375|Toolebuc Formation|64778|6|Mentioned|p13|Cretaceous|Cretaceous|Pedirka and Simpson Desert Basins.||||||
18375|Toolebuc Formation|64820|5|Briefly described|pS6 Fig. 4|Late Albian|Late Albian|Of the Rolling Downs Group. Carbonaceous to calcareous silt-claystone with minor sandstones. Geological province: Weipa Sub-basin, Carpentaria Basin.||||||
18375|Toolebuc Formation|65238|5|Briefly described|p7 Fig. 8|Early Cretaceous|Early Cretaceous|Geological province: Eromanga Basin. Transgressive marine deposits.||||||
18375|Toolebuc Formation|65342|5|Briefly described|p9.|||Eromanga Basin. Max. thickness at least 52 m. Seen as having potential as an insulating layer for geothermal energy.||||Overlies Bulldog Shale. Is overlain by Oodnadatta Shale.|Limestone, calcareous bituminous shale.|
18375|Toolebuc Formation|65385|5|Briefly described|pS134 Fig.7|Early Cretaceous|Early Cretaceous|Of Eromanga Basin. Overlies Wallumbilla Formation. Overlain by Allaru Mudstone.||||||08-MAR-12
18375|Toolebuc Formation|65489|5|Briefly described|p49, p55, p58, p96, p155|Early Cretaceous|Early Cretaceous|Eromanga Basin. 60m thick. Oil shale potential.||||Overlies Wallumbilla Formation. Is overlain by Allaru Mudstone.||
18375|Toolebuc Formation|66529|5|Briefly described|p10, p12, p16-17, p41, p92    |Mesozoic|Mesozoic|Eromanga Basin. Previously investigated for oil shale. An ideal in situ reductant for U systems.|c.107 Ma.|Unit in Rolling Downs Group.||Overlies Wallumbilla Formation. Is overlain by Allaru Mudstone.|Significant organic content. Black shale.|
18375|Toolebuc Formation|66623|6|Mentioned|p264.|||||||Is overlain by Allaru Mudstone.||
18375|Toolebuc Formation|66915|5|Briefly described|p6 Fig.3, p16|Cretaceous|Cretaceous|Eromanga and Carpentaria Basins. In later Rolling Downs Group units, the Toolebuc Formation is the only distinct and laterally persistent seismic reflection for correlation and is widespread in the Eromanga Basin.|||||Includes a thin competent unit of calcareous and bituminous shale, and limestone (a distinct and laterally persistent seismic reflection for correlation).|
18375|Toolebuc Formation|67323|5|Briefly described|p39, p81, p85-89, p93-94, p95 Fig.12.5|Early Cretaceous|Early Cretaceous|See also p96, GIS attrib tbl, Solid Geology Map. Eromanga/Carpentaria Basins. Oil shale was discovered in two wells (AAP Fermoy 1 and AAP Mayneside 1) in this unit by Australian Aquitaine Petroleum Pty Ltd in 1966. Attention shifted to outcrops in Julia Creek but activity ceased in 1969. Widespread shallow-marine deposits. Hydrocarbon exploration target in the Eromanga Basin; bituminous shale occurs throughout its extent. Considered prospective for U in the Carpentaria Basin.||||Overlies Wallumbilla Formation. Is overlain by Allaru Mudstone.|Calcareous bituminous shale, limestone.|
18375|Toolebuc Formation|67402|4|Described|p108, p109, p112|Albian|Albian|Eromanga Basin. Generally only between 20-45m thick but may be up to 65m thick. Deposited in a restricted marine environment. See also  p113 fig ERO12, p123, p176, p177, p179 fig CRP/KRM6, p180, p181.||Rolling Downs Group||Overlies the Wallumbilla Formation. Conformably overlain by the Allaru Mudstone.|Mudstone dominated succession that also contains limestone that is subordinate to calcareous, bituminous siltstone, labile sandstone and shale.|
18375|Toolebuc Formation|67561|6|Mentioned|p53 Fig.3|||||||||
18375|Toolebuc Formation|67784|5|Briefly described|p25-26, p28-29, p31-32, p34|Albian|Albian|6-25m thick. Carpentaria, northern Eromanga Basins. Appears as Toolebuc Limestone in Tb.1 (p28). Euxinic facies.||Wilgunya Subgroup.||Overlain by Allaru Mudstone. Overlies Ranmoor Member/Coreena Member (Wallumbilla Formation). Is correlated with Oodnadatta Formation|Contains distinctive Inoceramus coquinites and oil shale.|08-FEB-18
18375|Toolebuc Formation|67870|5|Briefly described|p46-47, p50-52|Late Cretaceous|Late Cretaceous|Hydrocarbon seal.|||||Shaly limestone, marl, organic-rich (10% TOC) limestone, sandstone.|
18375|Toolebuc Formation|68206|5|Briefly described|p31, 33|Albian|Albian|NE Eromanga Basin. See also reference to Toolebuc Limestone (p32).||||Overlies Ranmoor Member (Wallumbilla Formation). Is overlain by Allaru Formation.|Limestone; distinctive Inoceramus coquinites and oil shale.|
18375|Toolebuc Formation|68279|6|Mentioned|p19|||Galilee Basin stratigraphic cross-section, and mineralogy table.||||||
18375|Toolebuc Formation|68307|5|Briefly described|p92|Early Cretaceous|Early Cretaceous|Eromanga-Carpentaria Basin. Organic-rich. Forms a strong reflective seismic horizon.||||||
18375|Toolebuc Formation|68553|6|Mentioned|Map legend; schematic diagram.|Cretaceous|Cretaceous|Eromanga and Carpentaria Basins.||Unit in Rolling Downs Group.||Conformably overlies Wallumbilla Formation. Is overlain conformably by Allaru Mudstone.||
18375|Toolebuc Formation|68731|6|Mentioned|pp209-211|||||||||
18375|Toolebuc Formation|68734|5|Briefly described|p218 Fig.2|Albian|Albian|Eromanga Basin (NE). Shallow marine.||Of the Rolling Downs Group.||||
18375|Toolebuc Formation|68821|5|Briefly described|p292 Fig.1, p295, p296, p298|Cenomanian|Cenomanian|Lower Cretaceous age. Parallic to marine sediments. Contains ubiquitous disseminated pyrite. Equivalent in age to the Surat Siltstone.|101 - 98 Ma|Of the Rolling Downs Group.|||Dominantly organic-rich black shale with thin (< 3 cm) beds of limestone.|
18375|Toolebuc Formation|69019|5|Briefly described|p85 Fig.21.|Albian|Albian|Southern Eromanga Basin.||||Overlies Oodnadatta and Wallumbilla Formations. Is overlain by Allaru Mudstone.||
18375|Toolebuc Formation|69023|6|Mentioned|p89 Fig.20, p99|Albian|Albian|||||||
18375|Toolebuc Formation|69056|6|Mentioned|Reference images sheet.|||Shown on the simplified surface geology map of the Quamby Project area.||||||
18375|Toolebuc Formation|69206|6|Mentioned|p2|Cretaceous|Cretaceous||||||Immature oil shale.|
18375|Toolebuc Formation|69297|5|Briefly described|p273, p274 fig 4. 3, p275|Upper Albian|Upper Albian|Carpentaria Basin. The carbonaceous mudstones are the best potential source rocks in the basin.||Rolling Downs Group||Overlies the Wallumbilla Formation. Overlain by the Allaru Mudstone.|Carbonaceous mudstone, siltstone and claystone.|
18375|Toolebuc Formation|69454|6|Mentioned|p38:3|||Eromanga Basin.||||||12-JUL-16
18375|Toolebuc Formation|69455|6|Mentioned|p39:4 Fig.39.3|Early Cretaceous|Early Cretaceous|||||||12-JUL-16
18375|Toolebuc Formation|69457|3|Fully described|p41:2-3;41:5 Fig.41.4;41:6-8,10-12,15-18|Albian|Albian|Casey (1959). Eromanga, Carpentaria Basins. Widespread occurrence in drillholes. Shallow-marine deposits. Up to 65m thick. This unit and the Allaru Mudstone are together equivalent to the middle and upper part of Oodnadatta Formation. Has a distinctive, strong gamma signature in wireline logs. Regarded as an oil shale in the NE part of the Basin in Qld. A rich oil-gas source rock, the mudstone typically has a high TOC, generally 9-20%, locally 35%, derived from planktonic algae and cyanobacterial mats; it is an attractive oil shale and unconventional petroleum exploration target. Contains diverse fossil assemblages.||Wilgunya Subgroup.||Conformably overlies Wallumbilla Formation. Is overlain conformably by Allaru Mudstone.|Dark grey to black mudstone which may be carbonaceous, calcareous or pyritic, with thin layers of siltstone; subordinate labile sandstone, limestone, marl and conglomerate.|12-JUL-16
18375|Toolebuc Formation|69582|5|Briefly described|p22, p25-p26, p29, p65-p66|Lower Cretaceous|Lower Cretaceous|Eromanga Basin. Deposited in a marine depositional environment. Intersected in GSQ Longreach 2 drillhole.||||Overlies the Wallumbilla Formation. Overlain by the Allaru Mudstone.|Mudstone.|
18375|Toolebuc Formation|69591|6|Mentioned|p101 Fig.2.96|||||||Overlies Wallumbilla Formation. Is overlain by Allaru Formation.||
18375|Toolebuc Formation|69594|4|Described|p518-519, p521-522, p526, p529-530, p533|Albian|Albian|See also p574. Carpentaria, Eromanga Basins. A thin, isochronous unit up to 65m thick; generally 20-45m. Represents maximum marine conditions within an epeiric basin system. Early late Albian. Contains oil shales; may also be prospective for shale gas. Has a distinct and strong gamma signature. Contains spectacular vertebrate fossils (listed).||Rolling Downs Group.||Overlies Wallumbilla Formation. Is overlain conformably by Allaru Mudstone.|Coquinitic limestone, nodular limestone, oil shale, kerigenous shale, with minor siltstone and labile sandstone.|
18375|Toolebuc Formation|69673|6|Mentioned|p12 t5, p159, p160, p164, p165|||Prospective for unconventional hydrocarbons. Potential oil/gas source rock.||Wilgunya Subgroup||Overlain by Allaru Mudstone, overlies Wallumbilla Formation|Mudstone with thin layers of siltstone and subordinate labile sandstone, limestone, marl and conglomerate.|
18375|Toolebuc Formation|69797|5|Briefly described|p17 Fig.2|Early Cretaceous|Early Cretaceous|Geol. Prov: Eromanga Basin. Presented in figure as Toolebuc Fm.||||||
18375|Toolebuc Formation|69946|3|Fully described|p23-26, p57, p94|Albian|Albian|Originally Toolebuc Member (Casey, 1959) of the Wilgunya Formation. Later upgraded to Toolebuc Limestone (Vine et al., 1967), then defined as Toolebuc Formation by Senior et al. (1975). Casey's type section, outcrop on the Boulia-Winton Road 7 miles (11.3km) E of the Hamilton Hotel, was replaced because of poor outcrop by Senior et al. (1975) by the interval 25.3 - 35.8 m in BMR Boulia 3A. A reference section was also assigned to Boulia 3 (25 - 36m). High gamma ray response: its role in identifying Wallumbilla Formation mis-correlations from Qld into SA is discussed. Up to 50m thick. Wireline log correlations.||||Conformably overlies Wallumbilla Formation. Passes laterally into Oodnadatta Formation. Is overlain conformably by Allaru Mudstone.|Black calcareous and carbonaceous mudstone with abundant fish remains; dark grey fossiliferous mudstone with coquinite comprising large bivalve shells; dark grey mudstone. Bituminous shales in the type section; local oil shale origins.|
18375|Toolebuc Formation|69947|5|Briefly described|p13 Fig.7.2|Early Cretaceous|Early Cretaceous|Eromanga Basin.||Marree Subgroup.||||
18375|Toolebuc Formation|69948|6|Mentioned|Fig.4.18|||Eromanga Basin.||||Overlies Wallumbilla Formation. Is overlain by Allaru Mudstone.||
18375|Toolebuc Formation|70354|5|Briefly described|Map legend|Cretaceous|Cretaceous|||Rolling Downs Group.||Overlies Wallumbilla Formation. Is overlain by Allaru Mudstone.|Calcareous bituminous shale and limestone.|
18375|Toolebuc Formation|70572|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|||Wilgunya Subgroup|||Calcareous bituminous shale and limestone.|20-JAN-22
18375|Toolebuc Formation|70574|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|||Wilgunya Subgroup|||Calcareous bituminous shale and limestone.|18-JAN-22
18375|Toolebuc Formation|70821|5|Briefly described|p21, p33, p80|Early Cretaceous|Early Cretaceous|Eromanga Basin. Absent in the southern Thomson region.||Rolling Downs Group.||Overlies Oodnadatta and Wallumbilla Formations. Is overlain by Allaru Mudstone.||
18375|Toolebuc Formation|70823|5|Briefly described|p25-p27, p43-p44, p78|Early Cretaceous|Early Cretaceous|Eromanga Basin. Up to 60m thick. Deposited in a restricted, stratified and anoxic marine environment. Hosts an oil shale source rock.||||Overlies the Wallumbilla Formation. Overlain by the Allaru Formation.||
18375|Toolebuc Formation|70824|5|Briefly described|p9|Cretaceous|Cretaceous|Eromanga Basin. Hosts oil shale source rocks.||||Overlies the Wallumbilla Formation. Overlain by the Allaru Mudstone.||
18375|Toolebuc Formation|70836|6|Mentioned|p474|Albian|Albian|||||Coeval with Griman Creek Formation.||
18375|Toolebuc Formation|70860|6|Mentioned|p281|||Great Artesian Basin.||||||
18375|Toolebuc Formation|71059|6|Mentioned|p6 Fig.5|||Eromanga Basin.||||||
18375|Toolebuc Formation|71321|6|Mentioned|p15|||Of Eromanga Basin.||||Overlies the Wallumbilla Formation. Overlain by the Allaru Mudstone.||24-OCT-19
18375|Toolebuc Formation|71342|3|Fully described|Ch4 p25, Ch5 p23-p25|Late Albian|Middle Albian|Eromanga Basin. Originally named by Casey (1959) the Toolebuc Member of the Wilgunya Formation. Vine et al (1967) subsequently upgraded the member to formation status as the Toolebuc Limestone. Senior et al (1975) redefined the Limestone as the Toolebuc Formation. The type section for this unit was originally assigned to outcrop on the Boulia-Winton Road by Casey (1959). The BMR defined a new type section in Boulia 3A due to poor outcropping of the original section. A reference section was also given. Distribution and wireline log characteristics are given. A maximum thickness of 50m is recorded in Haddon Downs 1 in the northern Cooper region. Age derived from fossil assemblage and palynological studies. Interpreted to have been deposited in a restricted marine environment. Spore-pollen zone is given in Ch5 p57. See also Ch5 p57, Ch6 p9, Ch7 p13, Ch12 p12, Ch12 p14.||||Conformably overlies the Wallumbilla Formation. Conformably overlain by the Allaru Mudstone.|Black calcareous and carbonaceous mudstone with abundant fish remains, dark grey fossiliferous mudstone with coquinite containing abundant bivalves and bituminous shales.|
18375|Toolebuc Formation|71382|5|Briefly described|p4, p11, p13, p16-p17|||Eromanga Basin. Intersected in GSQ Julia 1 from 156.65m-199.87m for a total of 43.22m thickness. Deposited during widespread shallow marine conditions. Temp log and stratlog are provided. Lithology is described in detail on p21. See also p21, p23, p25, p27, App 3, 4.||||Overlies the Wallumbilla Formation. Overlain by the Allaru Mudstone.|Mudstone and calcareous mudstone.|
18375|Toolebuc Formation|71601|6|Mentioned|p120, p121|Albian|Albian|NW Qld. Includes dinosaur fossils provisionally assigned to Minmi.||||||
18375|Toolebuc Formation|71855|4|Described|p1-p2, p4-p6, p9-p11, p13, p15, p18, p20|Early Cretaceous|Early Cretaceous|Eromanga and Carpentaria basins. This unit has three distinct lithofacies which are described. In places the contact with the underlying Wallumbilla Formation is faulted or disconformable. This unit is highly organic rich and has good source rock charactersitcs. Wireline log responses were described for this unit including Gamma-ray, sonic transit time and resistivity. Structure, geochemistry and source rock potential are discussed. Typically greater than 15m thick. See also p22-p35, p42-p44, p47-p50, p52-p53, p56-p57, p61-p64, p66-p68, p73-p75.||Rolling Downs Group||Conformably (gradationally) overlies the Wallumbilla Formation. Conformably (gradationally) overlain by the Allaru Mudstone. Overlain by the Mackunda Formation.|Calcareous mudstone, coquinitic mudstone and organic-rich, slightly calcareous mudstone without calcite laminae.|
18375|Toolebuc Formation|71863|4|Described|p1-p18|Albian|Albian|Eromanga and Carpentaria basins. Originally defined as the Toolebuc Limestone by Vine et al. (1967). Subsequently this unit was redefined by Senior et al (1975) as the Toolebuc Formation due to recognition of significant mudstone component. The type section is defined in BMR Boulia 3A (Burger, 1974; Senior et al., 1975). Deposited during a marine incursion. Mudstone may contain laminae of carbonate form from bivalve remains Inoceramus and Aucellina (Ozimic, 1986). Deposited in a restricted, oxygen depleted marine environment. Wireline log characteristics, geochemistry, sedimentary facies, fossil assemblage, petroleum resources and mineralisation are discussed. Equivalent to the Wooldrige Limestone Member and Urisino beds.||Rolling Downs Group||Conformably overlies the Wallumbilla Formation. Conformably overlain by the Allaru Mudstone. Equivalent to the Wooldridge Limestone Member and Urisino beds.|Laminated calcareous and kerogenous mudstone, minor coquinite and limestone, labile sandstone and oil shale.|01-MAY-19
18375|Toolebuc Formation|72297|5|Briefly described|p712, p721, p728, p746, p751-753, p755|Early Cretaceous|Early Cretaceous|Eromanga and Carpentaria Basins. Julia Creek area; occurs north as far as 16 degrees S. Oxidised oil shales in the upper part produce soft oxide coquina, with associated large molybdenum and vanadium resources. Hosts a large gypsum deposit at Hughenden; other localities mentioned. An excellent though immature hydrocarbon source rock. Very high potential shale oil resources (perhaps the most extensive in Australia) despite very low grade; eg Julia Creek oil shale deposit (described).||||Conformably overlies the Ranmoor Member (Wallumbilla Formation). Is overlain conformably by the Allaru Mudstone.|A flat-lying unit comprising an upper, coarse limestone-clay-oil shale unit and a lower, fine carbonate-clay-oil shale unit. Contains mudstones rich in organic kerogenous material.|
18375|Toolebuc Formation|72298|5|Briefly described|p801|Cretaceous|Cretaceous|Eromanga Basin (SA,QLD,NSW), Carpentaria Basin.||Rolling Downs Group.||Overlies Coreena and Ranmoor Members (Wallumbilla FZ). Is overlain by Allaru Mudstone.||
18375|Toolebuc Formation|72799|6|Mentioned|p27|||||||||
18375|Toolebuc Formation|72913|6|Mentioned|p8.|||Three wells intersected this cover unit.||||||
18375|Toolebuc Formation|72967|6|Mentioned|p5|||Carpenteria Basin.||Rolling Downs Group||||
18375|Toolebuc Formation|73083|6|Mentioned|p58, p62-63|||||||Underlain by the Wallumbilla Formation.|Includes shale and subordinate limestone.|
18375|Toolebuc Formation|73137|6|Mentioned|p6|Cretaceous|Cretaceous|||||||
18375|Toolebuc Formation|73144|6|Mentioned|p8, p13|Cretaceous|Cretaceous|Carpentaria Basin. Aquitard with potential shale gas/oil play.||Rolling Downs Group||Underlain by Wallumbilla Formation. Overlain by Allaru Mudstone.||
18375|Toolebuc Formation|73147|5|Briefly described|p129|Aptian|Aptian|||Rolling Downs Group.||Overlies Wallumbilla Formation. Is overlain by Allaru Mudstone.||
18375|Toolebuc Formation|73167|6|Mentioned|p664 Fig. 2|Cretaceous|Cretaceous|Eromanga Basin.||||||
18375|Toolebuc Formation|73249|5|Briefly described|p319, p321, p323|Albian|Albian|Eromanga Basin. Deposited in a marine environment.||||Overlies the Wallumbilla Formation, underlies the Allaru Mudstone, lateral equivalent of the Coorikiana Sandstone.|Mudstone.|
18375|Toolebuc Formation|73251|6|Mentioned|p62|Early Cretaceous|Early Cretaceous|Eromanga Basin.||||Underlain by Wallumbilla Formation. Overlain by Allaru Mudstone. Equivalent to Oodnadatta Formation.||
18375|Toolebuc Formation|73281|6|Mentioned|Appendix (DIP)|||See DIP034_Petroleumdata.xlsx and DIP034_Welldata.xlsx.||||||
18375|Toolebuc Formation|73343|6|Mentioned|p337|Cretaceous|Cretaceous|Eromanga Basin.||||Underlain by Wallumbilla Formation. Overlain by Allaru Mudstone. Equivalent to Oodnadatta Formation.||
18375|Toolebuc Formation|73479|5|Briefly described|p156 Fig.2, p159|Cretaceous|Cretaceous|Eromanga Basin. Open shallow marine depositional environment.|ca 103 Ma|||Overlies Wallumbilla Formation, underlies Allaru Mudstone||
18375|Toolebuc Formation|73553|6|Mentioned|p7|Cretaceous|Cretaceous|||||||
18405|Toondi Formation|22663|5|Briefly described|S97-1 and 2 p3|Late Cretaceous|Early Cretaceous|||||||01-MAR-10
18405|Toondi Formation|22814|5|Briefly described|fig2|Cretaceous|Cretaceous|||||||
18405|Toondi Formation|41751|2|Defined|p2|Cenomanian|Albian|||||||
18405|Toondi Formation|42315|6|Mentioned|p2|Cenomanian|Albian|||||||
18405|Toondi Formation|42545|3|Fully described|p16|Cenomanian|Albian|Variation on Toondi Formation, WA.||||||
18405|Toondi Formation|43498|6|Mentioned|8|Santonian|Neocomian|||||||
18405|Toondi Formation|44133|5|Briefly described|p134|Cenomanian|Albian|Disconformably overlies Madura Formation. Disconformably overlain by Nurina Formation. Originally included in Madura Formation.||||||
18405|Toondi Formation|44145|4|Described|p549 fig 4-190, p553-4, p551, p554|Cenomanian|Albian|Eucla Basin. Type section in Transcontinental Railway 1 bore, Madura. Age from palynomorphs. Previously included in Madura Formation.||||Disconformably overlies Madura Formation.|Siltstone, claystone and shale. Minor sandstone; commonly pyritic.|
18405|Toondi Formation|61197|5|Briefly described|p473, p475, p478 Fig.4|Middle Cretaceous|Middle Cretaceous|Eucla Basin. Low-energy marine deposits. 0-60m thick.|||||Silt, clay/shale; minor sand; pyritic.|
18405|Toondi Formation|61630|6|Mentioned|p555 Fig. 3|Turonian|Albian|Geological Province: Eyre Sub-basin. Marine.||||||07-APR-09
18405|Toondi Formation|63124|5|Briefly described|p72|||Marine deposits. Geological Province: Bight Basin. Equivalent to Eumeralla Formation.||||||
18405|Toondi Formation|68715|6|Mentioned|p30 Fig.5|Cenomanian|Aptian|Bight Basin.||||||
18405|Toondi Formation|69297|5|Briefly described|p14 fig 2.4, p25 fig 2.9, p60|Turonian|Albian|Eyre Sub-basin.||||Equivalent to the Ceduna and Platypus Formations.|Shale.|
18446|Torrens Group|29780|6|Mentioned|p18|||||||||
18446|Torrens Group|30381|6|Mentioned|p222|||||||||
18446|Torrens Group|38004|6|Mentioned|Table 1|||||||||
18446|Torrens Group|41401|6|Mentioned|p29|||||||||
18446|Torrens Group|41404|5|Briefly described|p98|||||||||
18460|Torrowangee Group|22553|5|Briefly described|p77,p83|||part of the Adelaidean sequence||||||
18460|Torrowangee Group|22646|6|Mentioned|Fig 4 on p 102|||Adelaide Geosyncline (East).||||||
18460|Torrowangee Group|22730|5|Briefly described|p558 Fig1||Neoproterozoic|||||||
18460|Torrowangee Group|22772|5|Briefly described|p63,66,Table13.1|Neoproterozoic III|Cryogenian|||||||
18460|Torrowangee Group|22857|5|Briefly described|p64, Tb. 13.1 (insert p70-71)|Marinoan|Sturtian|Geological Province: Adelaide Fold Belt. See also p398 and 400 App. 1 Tb.A1.3.||||||
18460|Torrowangee Group|23833|6|Mentioned|p256 fig.2|||||||||
18460|Torrowangee Group|29864|6|Mentioned|p263|||||||||
18460|Torrowangee Group|29921|6|Mentioned|Fig.1|||||||||
18460|Torrowangee Group|29991|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
18460|Torrowangee Group|30261|6|Mentioned|Table 1|||Willouran to Marinoan||||||
18460|Torrowangee Group|30683|6|Mentioned|Table 1|||||||||
18460|Torrowangee Group|30908|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|Probable Adelaide System equivalent.||||||
18460|Torrowangee Group|31012|6|Mentioned|p8|||Adelaidean. Lithology.||||||
18460|Torrowangee Group|32671|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
18460|Torrowangee Group|33004|6|Mentioned|Fig.8|||||||||
18460|Torrowangee Group|33468|6|Mentioned|p210|||||||||
18460|Torrowangee Group|33729|4|Described|p82|||U.Prot.||||||
18460|Torrowangee Group|33730|6|Mentioned|p191|||Late Precambrian||||||
18460|Torrowangee Group|33734|6|Mentioned|p494|||||||||
18460|Torrowangee Group|33875|6|Mentioned|p22|||Uranium deposit||||||
18460|Torrowangee Group|34468|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|Equivalents||||||
18460|Torrowangee Group|34469|6|Mentioned|p105|||Table. See also PP109,110 etc. Upper Proterozoic||||||
18460|Torrowangee Group|34563|6|Mentioned|p58|||Structure||||||
18460|Torrowangee Group|34812|6|Mentioned|p4|||See also P53||||||
18460|Torrowangee Group|34814|6|Mentioned|Fig.2|||||||||
18460|Torrowangee Group|35199|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
18460|Torrowangee Group|36411|6|Mentioned|p270|||Refs Cooper et al. 1978 for definition.||||||
18460|Torrowangee Group|36733|6|Mentioned|Table 5|||||||||
18460|Torrowangee Group|37627|6|Mentioned|p185|||||||||
18460|Torrowangee Group|37931|6|Mentioned|p531|||||||||
18460|Torrowangee Group|38969|6|Mentioned|p199|||||||||
18460|Torrowangee Group|39214|5|Briefly described|p7|||||||||
18460|Torrowangee Group|39574|6|Mentioned|p155|||||||||
18460|Torrowangee Group|39652|6|Mentioned|p5|||||||||
18460|Torrowangee Group|39885|6|Mentioned|p427|||||||||
18460|Torrowangee Group|40595|6|Mentioned|p91|||||||||
18460|Torrowangee Group|41403|6|Mentioned|Table 5|||||||||
18460|Torrowangee Group|41405|5|Briefly described|p203|||||||||
18460|Torrowangee Group|41801|6|Mentioned|Fig.4|||||||||
18460|Torrowangee Group|42531|5|Briefly described|Map legend|Adelaidean||||||||
18460|Torrowangee Group|42982|5|Briefly described|Table 1,p333|||||||||
18460|Torrowangee Group|43192|6|Mentioned|Table1 p61|||||||||
18460|Torrowangee Group|43263|6|Mentioned|Map Legend||Neoproterozoic|||||||
18460|Torrowangee Group|43265|5|Briefly described|Map Legend||Neoproterozoic|||||||
18460|Torrowangee Group|43268|5|Briefly described|Map Legend||Neoproterozoic|||||||
18460|Torrowangee Group|43269|5|Briefly described|Map Legend||Neoproterozoic|||||||
18460|Torrowangee Group|43357|14|Not recorded|155-161||Neoproterozoic|||||||
18460|Torrowangee Group|43383|14|Not recorded|p3-6|Permian|Carboniferous|||||||
18460|Torrowangee Group|43464|14|Not recorded|Map Legend||Neoproterozoic|(Provisional Edition)||||||
18460|Torrowangee Group|43501|14|Not recorded|Map Legend||Neoproterozoic|(Provisional Edition)||||||
18460|Torrowangee Group|43502|14|Not recorded|Map Legend||Neoproterozoic|(Provisional Edition)||||||
18460|Torrowangee Group|44093|5|Briefly described|p110|Neoproterozoic|Neoproterozoic|See also p139 Appendix 1. Geological Province: Adelaide Fold Belt.||||||29-MAR-05
18460|Torrowangee Group|46889|6|Mentioned|p277|||||||||
18460|Torrowangee Group|48926|6|Mentioned|p67|||P67 et seq.||||||
18460|Torrowangee Group|60648|5|Briefly described|p41 Fig. 1|Neoproterozoic|Neoproterozoic|Unconformably overlies the Willyama Series of rocks.  Geological Province: Darling Basin.||||||28-APR-05
18460|Torrowangee Group|62724|5|Briefly described|p17 Fig. 4|Sturtian|Sturtian|Includes the Yancowinna Subgroup. Geological Province: Broken Hill Domain.||||||07-FEB-11
18460|Torrowangee Group|66623|5|Briefly described|p13, p17.|||Name replaced Torrowangee Series of Mawson (1912).|||Includes Teamsters Creek Subgroup.|Overlain by Kara Formation of Grey Range Group.|Wide variety of meta-sandstone, green-grey meta-siltstone, brown calcareous sandstone, grey quartzite, conglomerates, diamictite, dolomite, flaggy limestone and pyritic shale.|
18460|Torrowangee Group|67562|6|Mentioned|p102 Fig.8|Precambrian|Precambrian|||||||
18460|Torrowangee Group|70000|5|Briefly described|p32-34, p39|Ediacaran|Cryogenian|Syn-rift deposition in the Broken Hill area resumed following Sturtian tectonism. Hosts two glacially-distributed glacial successions separated by carbonate-rich interglacial deposits. Mis-spelt as Tarrowangee on p32-33 and p41.|||Includes Yancowinna, Euriowie and Teamsters Creek, Subgroups.|||
18460|Torrowangee Group|70013|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Burta (geophysical basement) Zone. Three facies are mapped separately: dominantly quartzite and sandstone, dominantly siltstone and claystone, ironstone (magnetite/hematite-rich beds). Interpreted as continental and marine sediments that accumulated within intra-continental rift basins. Part of a sedimentary package that unconformably overlies the Broken Hill Block.|||||Quartzite, sandstone, siltstone, claystone, limestone, ironstone.|
18460|Torrowangee Group|70015|5|Briefly described|Map legend|Ediacaran|Cryogenian|Mineral deposits (if any) are shown. Also appears (mis-spelt) as Tarrowangee Group.|||Includes Yancowinna, Euriowie and Teamsters Creek Subgroups.|Is overlain by Farnell Group.|Sandstone, quartzite, siltstone, shale +/- pyrite, flaggy limestone, sandy limestone, dolomite, polymictic (para)conglomerate, diamictite, pebbly siltstone/mudstone.|
18473|Tortachilla Limestone|9124|5|Briefly described|Map Legend|Oligocene|Eocene|Glauconitic limestone. Underlies Blanche Point Marls.||||||
18473|Tortachilla Limestone|22525|6|Mentioned|p35,37||Eocene|Grouped as Undifferentiated Blanche Point Formation and Tortachilla Limestone in this paper.||||||12-DEC-06
18473|Tortachilla Limestone|22528|4|Described|p42 p45-6||Late Eocene|||||||
18473|Tortachilla Limestone|22541|4|Described|p 21 22, Fig 1, 7||Middle Eocene|Blanche Point Formation||||||
18473|Tortachilla Limestone|22587|6|Mentioned|p79 Fig.7|Late Eocene|Late Eocene|||||||
18473|Tortachilla Limestone|23331|5|Briefly described|1089 Fig.2|Eocene|Eocene|||||||
18473|Tortachilla Limestone|23489|4|Described|p44|Oligocene|Eocene|||||||
18473|Tortachilla Limestone|23768|5|Briefly described|p28 Fig.5, p103, p105|Late Eocene|Late Eocene|Geological Province: St Vincent Basin.  See also p78, p101,  p103, p105, p123.||||||29-MAR-05
18473|Tortachilla Limestone|23802|5|Briefly described|p21 Fig. 2|||Glauconitic ferruginous fossiliferous limestone; includes oyster shells.||||||
18473|Tortachilla Limestone|23818|5|Briefly described|p174 Fig.84, p188|Late Eocene|Late Eocene|Geological Province: St. Vincent Basin. Max. thickness: 100 ft.||||||
18473|Tortachilla Limestone|23828|5|Briefly described|p94|Late Eocene|Late Eocene|Geological Province: St Vincent Basin. Maximum thickness: 30m.||||||
18473|Tortachilla Limestone|29355|6|Mentioned|p185|||||||||
18473|Tortachilla Limestone|29591|6|Mentioned|p103|||||||||
18473|Tortachilla Limestone|29601|6|Mentioned|p82|||||||||
18473|Tortachilla Limestone|29665|6|Mentioned|p79|||||||||
18473|Tortachilla Limestone|30014|4|Described|p33|||In Appendix.||||||
18473|Tortachilla Limestone|30250|6|Mentioned|p2|||Also mention Table 2 and Fig.2.||||||12-DEC-06
18473|Tortachilla Limestone|30251|6|Mentioned|p3|||Table on p3.||||||12-DEC-06
18473|Tortachilla Limestone|30828|6|Mentioned|p113|||||||||
18473|Tortachilla Limestone|31515|6|Mentioned|Text Fig.1|||||||||
18473|Tortachilla Limestone|31922|6|Mentioned|p173|||||||||
18473|Tortachilla Limestone|31923|6|Mentioned|p17|||||||||
18473|Tortachilla Limestone|32117|6|Mentioned|Fig.2|||||||||
18473|Tortachilla Limestone|32119|6|Mentioned|p481|||||||||
18473|Tortachilla Limestone|32509|5|Briefly described|p9|||From drillhole||||||
18473|Tortachilla Limestone|32552|6|Mentioned|p183|||U.Eocene. See also p185.||||||12-DEC-06
18473|Tortachilla Limestone|33057|6|Mentioned|p8|||Equivalents mentioned.||||||
18473|Tortachilla Limestone|34295|5|Briefly described|p32|||||||||
18473|Tortachilla Limestone|34308|4|Described|p188|||M.Eocene. Cor. chart Fig.84||||||
18473|Tortachilla Limestone|34421|6|Mentioned|p255|||Upper Eocene. See also p269,271.||||||12-DEC-06
18473|Tortachilla Limestone|34898|6|Mentioned|Table 1|||||||||
18473|Tortachilla Limestone|35689|2|Defined|p16|late Eocene|late Eocene|||||||
18473|Tortachilla Limestone|35697|6|Mentioned|p90|||||||||
18473|Tortachilla Limestone|36119|6|Mentioned|p47|||||||||
18473|Tortachilla Limestone|36127|5|Briefly described|p9|||See also p7.||||||12-DEC-06
18473|Tortachilla Limestone|36200|6|Mentioned|Table 1|||||||||
18473|Tortachilla Limestone|36244|6|Mentioned|p2|||Redefined by Cooper 1979.||||||
18473|Tortachilla Limestone|36490|6|Mentioned|p189|||||||||
18473|Tortachilla Limestone|37324|6|Mentioned|p11|||||||||
18473|Tortachilla Limestone|38068|6|Mentioned|Fig.7|||||||||
18473|Tortachilla Limestone|38107|4|Described|p25|||||||||
18473|Tortachilla Limestone|38621|1|Redefined|p3|late Eocene|late Eocene|||||||
18473|Tortachilla Limestone|38699|6|Mentioned|p8|||||||||
18473|Tortachilla Limestone|38702|6|Mentioned|p127|||||||||
18473|Tortachilla Limestone|38773|6|Mentioned|p44|||||||||
18473|Tortachilla Limestone|38873|4|Described|p29|||||||||
18473|Tortachilla Limestone|39351|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
18473|Tortachilla Limestone|40003|5|Briefly described|Table 11|||See also p47.||||||12-DEC-06
18473|Tortachilla Limestone|40148|5|Briefly described|p161|||||||||
18473|Tortachilla Limestone|40152|6|Mentioned|Fig.3|||||||||
18473|Tortachilla Limestone|40238|6|Mentioned|p324|||||||||
18473|Tortachilla Limestone|40429|6|Mentioned|Fig.2|||||||||
18473|Tortachilla Limestone|40442|4|Described|p26|||||||||
18473|Tortachilla Limestone|40453|6|Mentioned|p61|||||||||
18473|Tortachilla Limestone|40778|6|Mentioned|p536|||||||||
18473|Tortachilla Limestone|40877|5|Briefly described|p47|||||||||
18473|Tortachilla Limestone|40969|5|Briefly described|p7|||||||||
18473|Tortachilla Limestone|40970|6|Mentioned|p16|||||||||
18473|Tortachilla Limestone|41025|6|Mentioned|Fig.2|||||||||
18473|Tortachilla Limestone|41076|6|Mentioned|p70|||||||||
18473|Tortachilla Limestone|41495|4|Described|p43|||||||||
18473|Tortachilla Limestone|41513|6|Mentioned|p43|||||||||
18473|Tortachilla Limestone|41517|6|Mentioned|p135|||||||||
18473|Tortachilla Limestone|41520|5|Briefly described|Fig.6|||||||||
18473|Tortachilla Limestone|41626|6|Mentioned|p50|||||||||
18473|Tortachilla Limestone|42371|6|Mentioned|p39, p44|Eocene||||||||
18473|Tortachilla Limestone|42443|6|Mentioned|p7|||In the St Vincent Basin.||||||12-DEC-06
18473|Tortachilla Limestone|42498|5|Briefly described|Map Legend|Eocene|Eocene|||||||
18473|Tortachilla Limestone|42506|5|Briefly described|Map legend|Eocene||Age Tertiary||||||
18473|Tortachilla Limestone|42574|6|Mentioned|Fig.2 P242|||||||||
18473|Tortachilla Limestone|42655|6|Mentioned|p46|||||||||
18473|Tortachilla Limestone|42733|5|Briefly described|map legend|Tertiary||||||||
18473|Tortachilla Limestone|44133|5|Briefly described|p167, 165 Fig. 10.11|Late Eocene|Middle Eocene|Geological Province: Saint Vincent Basin.||||||
18473|Tortachilla Limestone|46979|6|Mentioned|p109|||||||||
18473|Tortachilla Limestone|60538|5|Briefly described|p479 Fig. 18|Oligocene|Eocene|Geological Province: Saint Vincent Basin.||||||
18473|Tortachilla Limestone|60958|5|Briefly described|Map Legend|Eocene|Eocene|Limestone to sandy marl, locally glauconitic. Geological Province: Saint Vincent Basin.||||||
18473|Tortachilla Limestone|61121|5|Briefly described|Map legend|Eocene|Eocene|Limestone to sandy marl, locally glauconitic, with foraminifera. Geological Province: St. Vincent Basin.||||||06-JUN-05
18473|Tortachilla Limestone|61155|5|Briefly described|p17|Late Eocene|Late Eocene|Overlies Maslin Sands; overlain by Blanche Point Formation. Age: 40-38.5Ma. Max. thickness: 40m. Geological Province: St Vincent Basin.||||||12-DEC-06
18473|Tortachilla Limestone|64282|5|Briefly described|Map legend|Oligocene|Eocene|Geolocial Province: St Vincent Basin. Limestone to sandy marl, locally glauconitic, with foraminifera.||||||24-JUL-08
18473|Tortachilla Limestone|64397|5|Briefly described|p232 Fig. 1A, p233|Middle Eocene|Middle Eocene|Unconformable beneath Blanche Point Formation. Rubbly limestone, quartzose ferruginous sandy limestone. Geological province: St Vincent Basin. See also p233 Fig. 2.||||||
18473|Tortachilla Limestone|65375|6|Mentioned|p34 Fig.7, p35.|Eocene|Eocene|No outcrop on Yorke Peninsula. Contains foraminifera of Late Eocene age. Correlates with lower Muloowurtie Formation.||||||
18473|Tortachilla Limestone|65891|5|Briefly described|p221, p222 Fig.7, p226, p228 Fig.11.|Paleogene|Paleogene|St. Vincent Basin. Underlies Blanche Point Formation. Contains diverse neritic carbonate biota including echinoids, mollusks and bryozoans. Upper part is very thin, glauconitic, Spirocolpus-rich facies.||||||
18473|Tortachilla Limestone|66131|6|Mentioned|p242 Fig.2|Eocene|Eocene|Late Eocene in age (from Fig.2 - stratigraphic correlation chart).||||||
18473|Tortachilla Limestone|66194|5|Briefly described|p584-5||Eocene|St Vincent Basin. Marine. Late Eocene.||||||09-MAR-12
18473|Tortachilla Limestone|67462|5|Briefly described|Map legend.|Eocene|Eocene|Saint Vincent Basin.||||||
18473|Tortachilla Limestone|68715|6|Mentioned|p31 Fig.5|Bartonian|Lutetian|St Vincent Basin.||||||
18473|Tortachilla Limestone|70660|4|Described|p3, p7-p12, p15-p16, p19, p25-p27, p33|Early Priabonian|Late Bartonian|Also referred to in the past as the "Lower Member", "Upper Member", "Glauconitic Limestone Member" or the "Polyzoal Limestone Member." Lithology of both the upper and lower parts of this limestone are discussed in p9.||||Overlies the South Maslin Sand. Overlain by the Tuketja Member.|Bryozoan goethitic sands grading upwards into richly fossiliferous limestone that contains highly diverse molluscs and bryozoans.|
18473|Tortachilla Limestone|70722|5|Briefly described|p218,227|Middle Eocene|Middle Eocene|Of St. Vincent Basin. Equivalent to Kingscote Limestone Unit K1 of this study. Thin transgressive unit.||||Overlain by Blanche Point Formation. Underlain by South Maslin Sand.|Bryozoan carbonate.|
18473|Tortachilla Limestone|71787|6|Mentioned|p96 |||||||||
18473|Tortachilla Limestone|71789|6|Mentioned|p100|||South Australia.||||||
18473|Tortachilla Limestone|72450|5|Briefly described|Brochure map|Eocene|Eocene|||||||
18473|Tortachilla Limestone|73107|5|Briefly described|Map legend.|Eocene|Eocene||||||Limestone to sandy marl, locally glauconitic, with foraminifera.|
18473|Tortachilla Limestone|73188|5|Briefly described|p319-320, p345, p351|Middle Eocene|Middle Eocene|St Vincent Basin. Deposited in a fully marine environment. Records renewed transgression under warm marine conditions.||||Underlain by South Maslin Sand. Overlain by Blanche Point Formation.|Glauconitic limestone.|
18515|Townsend Quartzite|22496|6|Mentioned|p10||Neoproterozoic|In the Officer Basin.||||||12-DEC-06
18515|Townsend Quartzite|22716|6|Mentioned|table4, p238|Cryogenian|Cryogenian|Age: 830 Ma. Part of sequence 1 of Centralian Superbasin.||||||
18515|Townsend Quartzite|22816|5|Briefly described|p10 Fig. 4|Neoproterozoic|Neoproterozoic|Central Officer Basin||||||
18515|Townsend Quartzite|23282|6|Mentioned|p50|||May be a synonym of Pindyin Sandstone.||||||
18515|Townsend Quartzite|23288|5|Briefly described|p137|||||||||
18515|Townsend Quartzite|23557|5|Briefly described|p95 Fig.1|Cryogenian|Cryogenian|Geological Province: Officer Basin.||||||
18515|Townsend Quartzite|23571|4|Described|p7|Neoproterozoic|Neoproterozoic|Geological Province: Officer Basin. Unconformably underlain by Musgrave Complex. Disconformably overlain by Lefroy Formation and Browne Formation.||||||12-DEC-06
18515|Townsend Quartzite|23621|5|Briefly described|p33|||Geological Province: Officer Basin.||||||
18515|Townsend Quartzite|24067|5|Briefly described|p251|Adelaidean|Adelaidean|Geological Province: Officer Basin.||||||
18515|Townsend Quartzite|24161|4|Described|p6, p27|Neoproterozoic|Neoproterozoic|Unconformably overlies the Mission Group. Overlain by the Lefroy Formation. Geological Province: Officer Basin.||||||
18515|Townsend Quartzite|24173|5|Briefly described|p24|Neoproterozoic|Neoproterozoic|Part of extensive sand blanket which includes Mount Kinahan Sandstone, Vaughan Springs Quartzite, Heavitree Quartzite and Lewis Range Sandstone (Redcliff Pound Group).  Geological Province: Officer Basin.||||||12-DEC-06
18515|Townsend Quartzite|24244|6|Mentioned|p3|Neoproterozoic|Neoproterozoic|Officer Basin.||||||
18515|Townsend Quartzite|24390|5|Briefly described|p11 Fig. 6|Neoproterozoic|Neoproterozoic|Geological Province: Officer Basin. Age: ~ 800 Ma.||||||
18515|Townsend Quartzite|30218|6|Mentioned|p404|||||||||
18515|Townsend Quartzite|30385|6|Mentioned|p8|||Also Table 1||||||
18515|Townsend Quartzite|30386|4|Described|p7|||Table 1 p7. Proterozoic age.||||||12-DEC-06
18515|Townsend Quartzite|30388|6|Mentioned|p9|||Middle Proterozoic age||||||
18515|Townsend Quartzite|30390|4|Described|p81|||See also p82-84.||||||12-DEC-06
18515|Townsend Quartzite|30942|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
18515|Townsend Quartzite|30944|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
18515|Townsend Quartzite|30946|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Part of Bentley Supergroup||||||
18515|Townsend Quartzite|30947|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
18515|Townsend Quartzite|31457|4|Described|Table 2|||Mention p6.||||||12-DEC-06
18515|Townsend Quartzite|31460|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
18515|Townsend Quartzite|31632|4|Described|Table 2|||See also p10.||||||12-DEC-06
18515|Townsend Quartzite|31635|6|Mentioned|Table 2|||||||||
18515|Townsend Quartzite|31636|6|Mentioned|Table 2|||||||||
18515|Townsend Quartzite|31914|1|Redefined|p95|Neoproterozoic|Mesoproterozoic|Middle to Upper ProterozoicM - U.||||||24-SEP-08
18515|Townsend Quartzite|31967|6|Mentioned|p.4|||||||||
18515|Townsend Quartzite|31973|6|Mentioned|p3|||Refers Lowry et al. (1971)||||||
18515|Townsend Quartzite|32727|5|Briefly described|p10|||Strat. and dates.||||||12-DEC-06
18515|Townsend Quartzite|33468|6|Mentioned|p212|||See also p214.||||||12-DEC-06
18515|Townsend Quartzite|33478|6|Mentioned|p454|||||||||
18515|Townsend Quartzite|34917|6|Mentioned|p12|||||||||
18515|Townsend Quartzite|35308|6|Mentioned|p454|||||||||
18515|Townsend Quartzite|36096|6|Mentioned|Fig.3|||||||||
18515|Townsend Quartzite|36701|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
18515|Townsend Quartzite|36886|4|Described|p197|||||||||
18515|Townsend Quartzite|36888|4|Described|p216|||||||||
18515|Townsend Quartzite|37299|6|Mentioned|Fig.1|||||||||
18515|Townsend Quartzite|37460|4|Described|p176|||||||||
18515|Townsend Quartzite|37707|6|Mentioned|p24|||||||||
18515|Townsend Quartzite|38157|6|Mentioned|Table VIII|||||||||
18515|Townsend Quartzite|38898|6|Mentioned|p83|||||||||
18515|Townsend Quartzite|39120|6|Mentioned|p146|||||||||
18515|Townsend Quartzite|39565|6|Mentioned|p31|||||||||
18515|Townsend Quartzite|40309|6|Mentioned|p91|||||||||
18515|Townsend Quartzite|41405|5|Briefly described|p205|||||||||
18515|Townsend Quartzite|43442|6|Mentioned|p17,19||Neoproterozoic|Age: c.820 Ma (Korsch & Kennard,1991).||||||12-DEC-06
18515|Townsend Quartzite|43692|6|Mentioned|p144|||||||||
18515|Townsend Quartzite|43697|6|Mentioned|p28|||||||||
18515|Townsend Quartzite|43732|6|Mentioned|p3|||||||||
18515|Townsend Quartzite|43756|6|Mentioned|p541|||||||||
18515|Townsend Quartzite|44109|5|Briefly described|p81, p164|||Of the Bentley Supergroup. Overlies the Tollu Group. Unconformably overlies the Musgrave Block units.  Possibly equivalent to Heavitree Quartzite.||||||
18515|Townsend Quartzite|44111|6|Mentioned|p.58|||in Officer Basin. Is lithologically similar to Coondra Formation (Savory Basin) and Googhenama Formation (Paterson Orogen).||||||
18515|Townsend Quartzite|44139|5|Briefly described|p286, 284, 285 Fig.3-69|||Overlies Musgrave-Mann Complex and Mission Group, Bentley Supergroup and also Scamp, Palgrave and Skirmish Hill (acid volcanic and granite) Cauldrons. Thick to thin-bedded flaggy sandstone overlain by coarse-grained, thick to very thick-bedded sandstone with large-scale cross-bedding.|| ||||06-MAR-18
18515|Townsend Quartzite|45149|2|Defined|p21|Proterozoic|Proterozoic|See also p3 and Table 1.||||||12-DEC-06
18515|Townsend Quartzite|45155|6|Mentioned|p18|||||||||
18515|Townsend Quartzite|46975|6|Mentioned|p83|||||||||
18515|Townsend Quartzite|49792|5|Briefly described|Fig.5|||||||||12-DEC-06
18515|Townsend Quartzite|49833|6|Mentioned|p8|||||||||
18515|Townsend Quartzite|50008|5|Briefly described|p46 Fig.3|Neoproterozoic||Of Tarcunyah Group. Geological Province: Officer Basin.||||||
18515|Townsend Quartzite|50085|5|Briefly described|p11 Fig. 6|Neoproterozoic|Neoproterozoic|Age: ~800Ma.  Geological Province: Officer Basin.||||||
18515|Townsend Quartzite|50204|6|Mentioned|p51|Neoproterozoic|Neoproterozoic|Of the Officer Basin.||||||
18515|Townsend Quartzite|50205|5|Briefly described|p59 Fig.1|Neoproterozoic|Neoproterozoic|Of Officer Basin.||Unit in Buldya Group.||Is overlain by Lefroy Formation conformably and locally unconformably.|Sandstone.|02-MAR-15
18515|Townsend Quartzite|61023|5|Briefly described|p15 Fig. 8|Neoproterozoic|Neoproterozoic|Age: ~800Ma. Geological Province: Officer Basin.||||||11-APR-08
18515|Townsend Quartzite|61272|5|Briefly described|p120, p123 Fig.4|||Unconformably overlies the Musgrave Complex and unconformably overlain by the Lefroy Group.||||||
18515|Townsend Quartzite|61560|5|Briefly described|p496|Neoproterozoic|Neoproterozoic|Contains the Skirmish impact structure.  Age is Early Neoproterozoic. On COOPER 1:250 000 sheet.||||||
18515|Townsend Quartzite|61732|5|Briefly described|p4 Fig. 3|Willouran|Willouran|Geological Province: central Officer Basin.||||||07-FEB-11
18515|Townsend Quartzite|62453|3|Fully described|p5 Fig. 3, 14|Cryogenian|Tonian|Of Buldya Gp. Geol. Prov: Officer Basin. Overlies: Bently Supergroup. Previous usage is Townsend Range Series, Townsend Fm, Townsend quartzite. Synonym with Pidyin Sandstone. Overlain by Lefroy Fm, Browne Fm. Sandstone. Uncon. overlies: Musgrave Cplx.||||||
18515|Townsend Quartzite|62987|5|Briefly described|p30|||Of the Buldya Group. Geological Province: Officer Basin.||||||
18515|Townsend Quartzite|63866|5|Briefly described|p202|||Musgrave Province.||Bentley Supergroup||||
18515|Townsend Quartzite|64103|5|Briefly described|p400 Fig. 3|Cryogenian|Cryogenian|Of Buldya Group. Geological Province: Officer Basin.||||||07-FEB-11
18515|Townsend Quartzite|64325|5|Briefly described|p82 Fig. 2|Neoproterozoic|Neoproterozoic|Basal unit of Supersequence 1. Conformably overlain by Lefroy Formation. Geological Province: western Officer Basin. Sandstone unit. Contains fluvial to nearshore marine sandstones.||||||11-JUL-13
18515|Townsend Quartzite|64580|4|Described|map legend||Neoproterozoic|Of Buldya Group. Laminated to very thick bedded, well-sorted, medium- to coarse-grained quartz arenite and feldspathic arenite; minor conglomerate and shale beds; medium- to large-scale cross-bedding.||||||09-DEC-08
18515|Townsend Quartzite|64625|6|Mentioned|p246|||Basal clastic sediments of the Centralian Superbasin.|>c.830 Ma.|||||
18515|Townsend Quartzite|64793|6|Mentioned|p283-285 figs 2,3,4; p291 fig 8|Cryogenian|Cryogenian|Of central Officer Basin. Age inferred from Fig.3.|c.840 -c.838 Ma.|||Is overlain unconformably by Browne Formation.||
18515|Townsend Quartzite|64796|6|Mentioned|p183 fig 2|Neoproterozoic|Neoproterozoic|Of Officer Basin||||||
18515|Townsend Quartzite|64797|6|Mentioned|p153 Fig.2|Cryogenian|Cryogenian|Officer Basin. Lithology/rank not shown on diagram.||||||
18515|Townsend Quartzite|64970|4|Described|p718, p719 Fig. 2, p721 Fig. 6|Neoproterozoic|Neoproterozoic|Is overlain by Lefroy, Browne, Hussar, Kanpa and Steptoe Formations in places. Massive, pink to white, very hard, quartz sandstone. Geological Province: Officer Basin.||||||
18515|Townsend Quartzite|65102|4|Described|p363,364, 365, 366, 367,372, Figs.4-43|Neoproterozoic|Neoproterozoic|Paterson Orogen (SE) and Officer Basin. 100-370m. Quartz to feldspathic arenite, shale beds; minor conglomerate; marine, mainly littoral-sublittoral with possible deltaic influence; unconformable over granitic basement; type section 38km E of Ainslie Gorge; date on underlying Tollu Volcanics: 1060+/-140 Ma.||||||
18515|Townsend Quartzite|65338|6|Mentioned|p59.|||Officer Basin. Correlated with Vaughan Springs Quartzite.||||||
18515|Townsend Quartzite|65363|6|Mentioned|p5 Fig.4, p11.|Neoproterozoic|Neoproterozoic|North-central Officer Basin.||Unit in Buldya Group.||||
18515|Townsend Quartzite|65365|5|Briefly described|p10 Fig. 4|Cryogenian|Cryogenian|Of Buldya Group. Central Officer Basin.||||||19-MAR-12
18515|Townsend Quartzite|65366|5|Briefly described|p23 Fig. 3|Cryogenian|Cryogenian|Of Buldya Group, central Officer Basin||||||
18515|Townsend Quartzite|65410|6|Mentioned|p72.|Neoproterozoic|Neoproterozoic|Western Officer Basin. May be equivalent to Heavitree Quartzite in the Amadeus Basin. Part of Supersequence 1.||||||
18515|Townsend Quartzite|65416|5|Briefly described|p137, p138 Fig.3, p140, p145.|Late Proterozoic|Late Proterozoic|Crops out along the southwest margin of the Musgrave Complex. Officer Basin. Lateral equivalent of Heavitree Quartzite (Amadeus Basin). Part of Sequence LP1A of Supersequence PL1. Transgressive: fluvial to shallow marine. Correlated with Glass Spring Formation in the Savory Sub-basin.||||Unconformably overlies Musgrave Complex. Is overlain by Browne Formation unconformably and conformably/gradationally by Lefroy Formation.|Orthoquartzite.|
18515|Townsend Quartzite|66281|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Officer Basin.|||||Laminated to very thickly-bedded, well-sorted, medium- to coarse-grained quartz arenite and feldspathic arenite; minor conglomerate and shale beds; medium- to large-scale cross-bedding.|
18515|Townsend Quartzite|66282|6|Mentioned|Map legend.|||Officer Basin. No outcrop on map; interpreted bedrock geology only.||||||
18515|Townsend Quartzite|67128|5|Briefly described|p33|||Represents the base of the Officer Basin at the SW edge of the Musgrave Province. Has distinctly different provenance from MacDougall Formation.|c.1134 Ma (maximum depositional age).|||||
18515|Townsend Quartzite|67195|5|Briefly described|p9 fig 5, p10, p19 tbl 1, p20, 40, 47|Neoproterozoic|Neoproterozoic|Western Officer Basin. Thermal conductivity of 4.45 W/mK. Basal unit of one well in this study. See also App 1.||||Overlain by Lefroy Formation, unconformably overlain by Browne Formation|Quartzite.|04-JAN-23
18515|Townsend Quartzite|67244|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Officer Basin. Described together with Lefroy Formation.||Unit in Buldya Group.|||Laminated to very thickly bedded, well-sorted, medium- to coarse-grained quartz arenite and feldspathic arenite; minor conglomerate and shale beds; medium- to large-scale cross-bedding.|21-NOV-13
18515|Townsend Quartzite|67375|6|Mentioned|p38 Table 1. |||||||Conformably overlies Mission Group.||
18515|Townsend Quartzite|67553|6|Mentioned|p40|Stenian|Stenian|Geological province: Musgrave Province, North Australian Craton. Of Talbot Sub-basin, Bentley Sub-basin.||||Underlain by Milesia Formation/Mission Group.||
18515|Townsend Quartzite|68270|5|Briefly described|p678|||Western Officer Basin.||||Overlain disconformably by Lupton Formation.||
18515|Townsend Quartzite|68733|6|Mentioned|p190|||Northern and western Officer Basin.||||||06-DEC-17
18515|Townsend Quartzite|68995|6|Mentioned|p19, p20|||Officer Basin.||||Overlies the Milesia Formation.||
18515|Townsend Quartzite|69003|6|Mentioned|p60|Neoproterozoic|Neoproterozoic|Officer Basin.||Buldya Group.||||
18515|Townsend Quartzite|69029|6|Mentioned|p329|Neoproterozoic|Neoproterozoic|Of Officer Basin.||||Overlain by Lefroy Formation.||
18515|Townsend Quartzite|69091|4|Described|p34-35, p43, p44, see comments|Neoproterozoic|Neoproterozoic|Basal unit of western Officer Basin, cropping out at northeastern edge of basin. It has limited distribution (not found in drillholes further southwest). Brought to present-day surface by reactivated Winduldarra Fault. See also p106 Fig.5.7a, p107 Fig.5.8a, p109 Fig.5.10, p182, p184.||Buldya Group||Overlies Bentley Supergroup; overlies Mission Group.||
18515|Townsend Quartzite|69153|5|Briefly described|GEOL_LUT_CSV files; Rocks.csv|Cryogenian|Neoproterozoic|Officer Basin, Centralian Superbasin. Lithology description shared with Lefroy Formation. Sample description includes: sandstone, pebbly sandstone and conglomerate.||Buldya Group|||Quartz arenite and feldspathic arenite; minor conglomerate and shale beds|
18515|Townsend Quartzite|70018|6|Mentioned|p240|||Officer Basin.||||||
18515|Townsend Quartzite|70134|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Officer Basin.||Buldya Group.|||Laminated to very thickly bedded, well-sorted, medium- to coarse-grained quartz arenite and feldspathic arenite; minor conglomerate and  shale beds; medium- to large-scale cross-bedding; commonly intensely silicified.|
18515|Townsend Quartzite|70137|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Officer Basin. The two facies are mapped separately.||Buldya Group.||Overlies Milesia Formation.|Laminated to very thickly bedded, well sorted, medium- to coarse-grained quartz arenite and feldspathic arenite, minor conglomerate and shale beds, commonly intensely silicified; poorly exposed cobble and boulder conglomerate, lesser sandstone.|
18515|Townsend Quartzite|70634|4|Described|100k_geologyp_lut.csv|Cryogenian|Cryogenian|Says age Cryogenian, 850-635 Ma inferred or biostratigraphic.|||||Laminated to very thickly bedded, well sorted, medium- to coarse-grained quartz arenite and feldspathic arenite; minor conglomerate and shale beds; medium- to large-scale cross-bedding; commonly intensely silicified|30-AUG-18
18515|Townsend Quartzite|70793|4|Described|GEOL_LUT_CSV files|Tonian|Tonian|Of Officer Basin (Phase 1), Centralian Superbasin. Events: Officer Basin Cenozoic diapirism (66-0.01 Ma); Delamarian Orogeny (520-505 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma). See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop_lut.csv.|1000-800 Ma (inferred)|Unit of Buldya Group.|||Laminated to very thickly bedded, well-sorted, medium- to coarse-grained quartz arenite and feldspathic arenite; vobble and boulder conglomerate, and shale beds; medium- to large-scale cross-bedding; commonly intensely silicified|
18515|Townsend Quartzite|71211|6|Mentioned|p235|||||||Conformably or unconformably overlies the Mission Group.||
18515|Townsend Quartzite|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.||Unit of Buldya Group.|||Laminated to very thick bedded, well-sorted, medium- to coarse-grained quartz arenite and feldspathic arenite; minor conglomerate and shale beds; medium- to large-scale cross-bedding.|
18515|Townsend Quartzite|71268|4|Described|GEOL_LUT_CSV files|Tonian|Tonian|Of Officer Basin (Phase 1), Centralian Superbasin. Events: Officer Basin Cenozoic diapirism (66-0.01 Ma); Delamerian Orogeny (520-505 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma). Deposited in braided fluvial to nearshore marine environments. Sample GSWA 189557 (quartz sandstone) yielded a weighted mean 207Pb/206Pb age of 1134+\-19 Ma, interpreted to be maximum depositional age of the sandstone. Sample GSWA 195237 (lithic sandstone) yielded a concordia age of 1134+\5 Ma, interpreted as maximum depositional age of the sedimentary protolith.See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 1m_geologyp12_lut.csv.|1000-800 Ma (inferred0|Unit of Buldya Group.||Lowermost unit of Buldya Group. Overalin by Lefroy Formation or Browne Formation. Underlain by Bentley Supergroup.|Laminated to very thickly bedded, well-sorted, medium- to coarse-grained quartz arenite and feldspathic arenite; cobble and boulder conglomerate and shale beds; medium- to large-scale cross-bedding; commonly intensely silicified|
18515|Townsend Quartzite|72094|4|Described|p4, p5|Neoproterozoic|Neoproterozoic|Officer Basin. Outcrops of NW-trending ridges in the Officer Basin. Misspelt(?) as Townshend Qtz on  p5||Unit of Buldya Group||Underlain by Mission Group apparently concordantly in Warburton area.|Laminated to very thick-bedded, well-sorted, medium to coarse-grained quartz arenite and feldspathic arenite.|
18525|Tragowel Member|2967|5|Briefly described|p35, 46-47, 49|||Macumber (1978). Loddon Plain, Murray Basin. Slightly deeper water deposit. Type section is 33m to 47m in the Meran 10 bore near Kerang. Up to 25m thick. On p46 the author gives contradictory accounts of its stratigraphic position. Appears as Tragowel Clay Member on p176.||Parilla Sand.|s|Overlies Kerang Sand Member and (locally) Loxton Sands. Is overlain by Wandella Sandstone.|A sequence of white clay and silt.|
18525|Tragowel Member|10010|5|Briefly described|p12 Fig. 3|Early Pliocene|Early Pliocene|Of Loxton-Parilla Sand. Geological Province: Murray Basin.||||||13-AUG-07
18525|Tragowel Member|22773|5|Briefly described|Fig24.8p352|Early Pliocene|Early Pliocene|||||||
18525|Tragowel Member|22782|6|Mentioned|p15|||||||||
18525|Tragowel Member|22799|5|Briefly described|p24 Fig.10|Early Pliocene|Early Pliocene|||||||
18525|Tragowel Member|22857|5|Briefly described|p352 Fig.24.8|Early Pliocene|Early Pliocene|Of Loxton-Parilla Sand? (relationship not clear in figure). Geological Province: Murray Basin.||||||
18525|Tragowel Member|22887|5|Briefly described|Fig.6 p13|Early Pliocene|Early Pliocene|||||||
18525|Tragowel Member|22893|5|Briefly described|fig4 p9|||||||||
18525|Tragowel Member|23884|5|Briefly described|p155 Fig. 13.2|Early Pliocene|Late Miocene|Geological Province: Murray Basin.||||||
18525|Tragowel Member|34757|6|Mentioned|p50|||||||||
18525|Tragowel Member|39329|6|Mentioned|Fig.1|||||||||
18525|Tragowel Member|40820|6|Mentioned|Fig.1|||||||||
18525|Tragowel Member|42134|6|Mentioned|Fig.3 P335|||||||||
18525|Tragowel Member|42966|2|Defined|Table 27, p172|Early Pliocene||of Loxton-Parilla Sands||||||
18525|Tragowel Member|43791|6|Mentioned|p372, Fig1|||||||||
18525|Tragowel Member|43804|6|Mentioned|Fig.2,p49|||||||||
18525|Tragowel Member|49040|6|Mentioned|Fig.6|||||||||
18525|Tragowel Member|60452|5|Briefly described|p37|Cenozoic|Cenozoic|Of the Parilla Sand. White clay and silt sequence. Overlies the Kerang Sand Member; overlain by the Wandella Sand Member. Max. thickness: 25m.||||||19-NOV-08
18525|Tragowel Member|65552|5|Briefly described|p5 Fig. 3|Early Pliocene|Early Pliocene|Of Loxton-Parilla Sands. Overlies Kerang Sand Member and underlies Wandella Sandstone Member.||||||
18525|Tragowel Member|66286|6|Mentioned|p179, 188|||Southern Murray Basin. Shoreface and shelf sediments.||Unit in Loxton-Parilla sands.||Overlies Kerang Sand Member. Is overlain by Wandella Sandstone Member.||
18525|Tragowel Member|67179|4|Described|p581|Pliocene|Miocene|Marine, regressive.||Of Loxton Sand||Overlies the Kerang Sand Member, underlies the Wandella Sandstone.|Silt-sized clear quartz grains in a white clay matrix; marine.|28-MAY-13
18525|Tragowel Member|72445|6|Mentioned|App.7 p7 Fig.4.|Pliocene|Miocene|Shown only on the 'Lithostratigraphy of Cenozoic sediments in the Murray Basin' (from Brown & Stephenson 1991).||||Shown as partially overlying the Kerang Sand Member and partially underlying the Loxton-Parilla Sands. Partially equivalent to Bookpurnong beds.|Shown as including silt.|
18532|Trainor Hill Sandstone|22746|5|Briefly described|Fig.3 p515|Middle Cambrian|Middle Cambrian|||||||
18532|Trainor Hill Sandstone|22922|5|Briefly described|34|||||||||
18532|Trainor Hill Sandstone|23282|1|Redefined|p79||Middle Cambrian|of Krieg (1973) and defined by Benbow (1982). May be equiv to part of 'Wirrildar beds' and Moodlatana Formation. Age: Middle Cambrian 516-510Ma. of Marla Group, Officer Basin.||||||
18532|Trainor Hill Sandstone|23288|6|Mentioned|Fig.5|Late Cambrian|Middle Cambrian|||||||
18532|Trainor Hill Sandstone|23524|5|Briefly described|p221 Fig. 3|Middle Cambrian|Middle Cambrian|||||||
18532|Trainor Hill Sandstone|24067|5|Briefly described|p242|Paleozoic|Paleozoic|Geological Province: Officer Basin.||||||07-NOV-08
18532|Trainor Hill Sandstone|24112|5|Briefly described|p254 Fig.2|Middle Cambrian|Middle Cambrian|Of the Marla Group. Geological Province: Officer Basin||||||
18532|Trainor Hill Sandstone|30544|6|Mentioned|p49|||||||||
18532|Trainor Hill Sandstone|30807|6|Mentioned|p102|||Suggested map symbol||||||
18532|Trainor Hill Sandstone|31455|6|Mentioned|p12|||||||||
18532|Trainor Hill Sandstone|31698|6|Mentioned|Map legend|Late Cambrian|Middle Cambrian|?Middle to Upper CambrianM? - U||||||
18532|Trainor Hill Sandstone|35628|4|Described|Table 3|||See also P14.||||||
18532|Trainor Hill Sandstone|36096|6|Mentioned|Fig.3|||||||||
18532|Trainor Hill Sandstone|36109|6|Mentioned|Fig.2|||||||||
18532|Trainor Hill Sandstone|36491|6|Mentioned|Fig.2|||||||||
18532|Trainor Hill Sandstone|36920|6|Mentioned|Table 1|||||||||
18532|Trainor Hill Sandstone|38022|6|Mentioned|Fig.4|||||||||
18532|Trainor Hill Sandstone|38329|1|Redefined|p205|Cambrian|Cambrian|||||||
18532|Trainor Hill Sandstone|39352|6|Mentioned|Map legend|Late Cambrian|Early Cambrian|Early to Late Cambrian||||||
18532|Trainor Hill Sandstone|40945|6|Mentioned|Fig.3|||||||||
18532|Trainor Hill Sandstone|41276|6|Mentioned|Fig.1|||||||||
18532|Trainor Hill Sandstone|43052|5|Briefly described|Fig.2.10|||||||||
18532|Trainor Hill Sandstone|43053|5|Briefly described|Map Legend|Cambrian|Cambrian|Of the Marla Group. Deltaic sandstone, siltstone and shale.||||||25-MAY-05
18532|Trainor Hill Sandstone|43258|5|Briefly described|Map Legend||Cambrian|||||||
18532|Trainor Hill Sandstone|43298|5|Briefly described|Map Legend||Cambrian|||||||
18532|Trainor Hill Sandstone|43657|6|Mentioned|Fig.3,p4||Cambrian|||||||
18532|Trainor Hill Sandstone|43690|6|Mentioned|Fig.2,p157||Cambrian|||||||
18532|Trainor Hill Sandstone|43732|6|Mentioned|Fig.4,p5||Middle Cambrian|||||||
18532|Trainor Hill Sandstone|43743|6|Mentioned|Fig.2,p33||Middle Cambrian|||||||
18532|Trainor Hill Sandstone|44109|5|Briefly described|p22 Fig. 19|Cambrian|Cambrian|Of the Marla Group. Geological Province: central Officer Basin.||||||
18532|Trainor Hill Sandstone|44133|4|Described|p39, 42, 4 Fig. 7.2|Middle Paleozoic|Early Paleozoic|Geological Province: Eastern Officer Basin. Of the Marla Group. Overlies: Apamurra Formation. Contact with Mount Johns Conglomerate. Underlies: Byilkaoora Formation.||||||07-NOV-08
18532|Trainor Hill Sandstone|45149|6|Mentioned|Table 1|||Page 15.||||||
18532|Trainor Hill Sandstone|49792|5|Briefly described|Fig.5|||||||||
18532|Trainor Hill Sandstone|60565|5|Briefly described|p20 Fig.3b|||Overlies the Apamurra Formation.||||||
18532|Trainor Hill Sandstone|60953|5|Briefly described|Map Legend|Cambrian|Cambrian|Deltaic sandstone, siltstone and shale; fan-delta conglomerate and sandstone.||||||
18532|Trainor Hill Sandstone|61108|5|Briefly described|map legend|Cambrian|Cambrian|Deltaic sandstone, siltstone and shale; fan-delta conglomerate and sandstone.||||||
18532|Trainor Hill Sandstone|61732|6|Mentioned|p79, p82 Fig. 33|Cambrian|Cambrian|Geological Province: Birksgate Sub-basin.||||||07-FEB-11
18532|Trainor Hill Sandstone|62570|5|Briefly described|p580 Figs. 2 and 3|Middle Cambrian|Middle Cambrian|Of the Marla Group. Geological Province: Officer Basin. Feldspathic sandstone.||||||13-SEP-18
18532|Trainor Hill Sandstone|65313|5|Briefly described|p577, p578 Fig 6, p 573 Fig. 2|Late Cambrian|Middle Cambrian|Previously dated ca 500 Ma, now confirmed as 'no younger than mid-Late Cambrian', paleosols identified in section in Byilkaoora 2 borehole - Officer Basin.||Of Marla Group.||Overlies Apamurra Formation.||26-MAR-12
18532|Trainor Hill Sandstone|67120|5|Briefly described|Map legend|Cambrian|Cambrian|||Marla Group|||Sandstone, red-brown, fine-grained, cross-bedded; siltstone to claystone, red, micaceous; basal very fine-grained sandstone.|
18532|Trainor Hill 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.|
18532|Trainor Hill Sandstone|67921|5|Briefly described|Map legend|Cambrian|Cambrian|Subcrop and minor outcrop.|||||Fine- to medium-grained, kaolinitic, micaceous and lithic white quartz sandstone; cross-bedded; soft sediment disruption including roll slumps; thin mudstone interbeds and locally some clay intraclasts.|
18532|Trainor Hill Sandstone|69445|5|Briefly described|p30:5, 17|||Officer Basin.||||Is overlain by Kulyong Formation (now Table Hill Volcanics).||12-JUL-16
18532|Trainor Hill Sandstone|70336|5|Briefly described|Map legend|Cambrian|Cambrian|||Of Marla Group.|||Red-brown, fine-grained, cross-bedded sandstone; red, micaceous siltstone to claystone; basal very fine-grained sandstone.|12-JAN-16
18532|Trainor Hill Sandstone|70839|5|Briefly described|p342-343,345|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.||
18532|Trainor Hill Sandstone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone|
18532|Trainor Hill Sandstone|71618|6|Mentioned|p130|||Of Officer Basin.||||||
18532|Trainor Hill Sandstone|72478|6|Mentioned|p8, p11|Middle Cambrian|Early Cambrian|Officer Basin. See also p51, 69, Fig.7 p70 [of the document].|c. 516 Ma-510 Ma|Marla Group||||29-MAR-21
18532|Trainor Hill Sandstone|73090|5|Briefly described|p12 Fig.7|Cambrian|Cambrian|||Marla Group.|||Sandstone, red-brown, fine-grained, cross-bedded; siltstone to claystone, red, micaceous; basal very fine-grained sandstone.|
18532|Trainor Hill Sandstone|73099|5|Briefly described|Map legend.|Middle Cambrian|Early Cambrian|Officer Basin.||Marla Group.||Overlies Apamurra Formation. Is overlain by Mount Chandler Sandstone (Munda Group).|Pale grey, white and yellow-brown, fine- to coarse-grained, micaceous, feldspathic quartz sandstone with numerous interbeds of green-grey and red-brown micaceous siltstone and claystone.|
18532|Trainor Hill Sandstone|73100|5|Briefly described|Map legend|Cambrian|Cambrian||||||Fine- to medium-grained, kaolinitic, micaceous and lithic white quartz sandstone; trough or angular cross-bedding; soft sediment disruption; thin mudstone interbeds, clay intraclasts locally.|
18532|Trainor Hill Sandstone|73109|5|Briefly described|Map legend.|Cambrian|Cambrian|Subcrop and minor outcrop.|||||Fine- to medium-grained, kaolinitic, micaceous and lithic white quartz sandstone, locally with red mottling or diffuse pale colourations; trough or angular cross-bedding; soft sediment disruption; thin mudstone interbeds; clay intraclasts locally.|
18532|Trainor Hill Sandstone|73111|5|Briefly described|Map legend.|Cambrian|Cambrian|Subcrop and minor outcrop.|||||Fine- to medium-grained, kaolinitic, micaceous and lithic white quartz sandstone, local red mottling or diffuse pale colourations; low angle trough or angular cross-bedding; soft sediment disruption; thin mudstone interbeds; local clay intraclasts.|
18582|Trezona Formation|22510|5|Briefly described|table1p37,41|||Of the Upalinna Subgroup.  Age: Marinoan. Central Flinders Ranges||||||08-JUL-13
18582|Trezona Formation|22911|6|Mentioned|37|||||||||
18582|Trezona Formation|23250|5|Briefly described|p1122, p1124  Fig.2||Cryogenian|of Umberatana Group. Correlate of Wilmington Formation equivalent and Olympic Formation.||||||
18582|Trezona Formation|23314|5|Briefly described|331 Fig.2|||||||||
18582|Trezona Formation|23394|5|Briefly described|Map legend|Proterozoic|Proterozoic|||||||
18582|Trezona Formation|23562|5|Briefly described|p295 Fig 2|Neoproterozoic III|Cryogenian|||||||
18582|Trezona Formation|23818|5|Briefly described|p64 Fig.22, p68|Neoproterozoic|Neoproterozoic|Uppermost unit of the Farina Sub-Group. Max thickness: 800 ft.||||||
18582|Trezona Formation|23913|4|Described|p110 Fig. 2|Adelaidean|Adelaidean|Geological Province: Central Flinders Zone.  Of the Umberatana Group.  Underlying Unit: Enorama Shale.  Overlying Unit: Elatina Formation.||||||
18582|Trezona Formation|24176|4|Described|p13, p24 Tb. 1|Adelaidean|Adelaidean|Of the Farina Sub-Group. Grey-green calcareous shales, breccia limestone or dolomite; stromatolites. Overlies Enorama Shale; underlies Fortress Hill  Formation.  Max. thickness: 185m. Age is Marinoan. Geological Province: Mount Painter Province.||||||30-SEP-08
18582|Trezona Formation|24195|6|Mentioned|p48|||||||||
18582|Trezona Formation|24476|4|Described|p547 Fig. 4|Vendian|Vendian|Overlies the Enorama Shale. Overlain by the Elatina Formation.  Geological Province: Adelaide fold belt.||||||
18582|Trezona Formation|29780|5|Briefly described|p40|||||||||
18582|Trezona Formation|30176|6|Mentioned|Map legend|Adelaidean|Adelaidean|Marinoan||||||
18582|Trezona Formation|30801|6|Mentioned|p5|||Marinoan. Table P5-6||||||
18582|Trezona Formation|30802|4|Described|Table 1|||Marinoan||||||
18582|Trezona Formation|32720|6|Mentioned|Table 1|||||||||
18582|Trezona Formation|32722|6|Mentioned|Fig.3|||Adelaidean. Stromatolite||||||
18582|Trezona Formation|32724|4|Described|p520|||Marinoan||||||
18582|Trezona Formation|33474|6|Mentioned|Fig.2|||||||||
18582|Trezona Formation|34175|6|Mentioned|p36|||||||||
18582|Trezona Formation|34267|6|Mentioned|Fig.|||The Oraparinna & Enorama diapiric structures.||||||
18582|Trezona Formation|34291|6|Mentioned|p13|||See also PP16,73. Adelaidean||||||
18582|Trezona Formation|34534|6|Mentioned|Fig.2.13|||||||||
18582|Trezona Formation|34535|4|Described|p69|||See also Fig.22||||||
18582|Trezona Formation|35075|6|Mentioned|p77|||||||||
18582|Trezona Formation|35255|6|Mentioned|Fig.7|||||||||
18582|Trezona Formation|36733|6|Mentioned|Table 5|||||||||
18582|Trezona Formation|37015|5|Briefly described|p67|||||||||
18582|Trezona Formation|37461|6|Mentioned|Table 5.I|||||||||
18582|Trezona Formation|37627|6|Mentioned|Fig.2|||||||||
18582|Trezona Formation|37932|6|Mentioned|p546|||||||||
18582|Trezona Formation|38157|6|Mentioned|Table IV|||||||||
18582|Trezona Formation|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Marinoan||||||
18582|Trezona Formation|40852|6|Mentioned|Fig.3.2|||||||||
18582|Trezona Formation|41405|3|Fully described|p186|||Mention p161 and p200||||||12-AUG-15
18582|Trezona Formation|42098|5|Briefly described|Table 2 P54|||||||||
18582|Trezona Formation|42222|6|Mentioned|p17|||||||||
18582|Trezona Formation|42239|5|Briefly described|p150|||||||||
18582|Trezona Formation|42542|6|Mentioned|Fig.4 P14|||||||||
18582|Trezona Formation|42882|5|Briefly described|Fig.7 P12, Table1 P3|||of Umberatana Group||||||
18582|Trezona Formation|43052|5|Briefly described|p189,Table 6.1|||||||||
18582|Trezona Formation|43845|5|Briefly described|Fig3 p43||Neoproterozoic|In Umberatana Group||||||12-JUL-16
18582|Trezona Formation|44659|5|Briefly described|map legend|||Marinoan, lithology.||||||
18582|Trezona Formation|46865|6|Mentioned|Table 2|||||||||
18582|Trezona Formation|60959|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Of the Upalinna Subgroup. Cycles of laminated greenish grey calcareous shale and siltstone grading to fine grained stromatolitic, oolitic and intraclastic hash breccia limestone.||||||
18582|Trezona Formation|61236|6|Mentioned|p24 Fig. 1|Adelaidean|Adelaidean|||||||
18582|Trezona Formation|61732|5|Briefly described|p28 Fig. 13|Marinoan|Marinoan|Of the Upalinna Subgroup (Umberatana Group). Geological Province: Adelaide Rift Complex.||||||07-FEB-11
18582|Trezona Formation|62085|6|Mentioned|p18, p20 fig 5, p21 fig 6|Cryogenian|Cryogenian|Pre-glacial.||||Is overlain by Yaltipena Formation.|Oolitic, stromatolitic and intraclastic limestones.|
18582|Trezona Formation|62592|5|Briefly described|p50 Table 5.1.|Marinoan|Marinoan|Adelaide Geosyncline.||Unit in Upalinna Subgroup.||Overlies Enorama Shale. Is overlain by Yaltipena Formation.|Limestone, siltstone.|
18582|Trezona Formation|62903|6|Mentioned|p729|||Interglacial. Date from Enorama Shale and Trezona Formation|690+/-21 Ma Rb-Sr whole-rock shale date, imprecise|||||
18582|Trezona Formation|64625|6|Mentioned|p256 |||Has negative d13C values, mostly between -10 and -4 parts per thousand.||||Overlain by Elatina Formation.||
18582|Trezona Formation|64797|5|Briefly described|p153 Fig.2, p161, p164 Fig.11. |||See also p166 Tb.7, p168 Tb.11, p169 Fig.12. Central Flinders Ranges. S-isotope data.||||||
18582|Trezona Formation|64801|5|Briefly described|p110 Fig.2, p112, p116|Neoproterozoic|Neoproterozoic|Adelaide Rift Complex.||Umberatana Group.|||Shallow-water limestones; large stromatolitic domes common.|
18582|Trezona Formation|64846|6|Mentioned|p203, p209|||Indicates that negative delta-13C values are not exclusively restricted to deeper-water carbonate lithologies.|||||Shallow-water carbonates: ooids, rip-up clasts, stromatolites; conspicuously red from synsedimentary haematite (to 17% of whole rock).|
18582|Trezona Formation|65892|5|Briefly described|p33 Fig.18, p36-37, p39. |Cryogenian|Cryogenian|Contains spectacular stromatolites.|c.630 Ma.|Unit in Umberatana Group.||Overlies Enorama Shale. Is overlain by Yaltipena Formation.|Shallow marine limestone and siltstone.|
18582|Trezona Formation|65925|5|Briefly described|Appendix 2.||||||||Limestone, intraclastic and stromatolitic; with interbeds of calcareous siltstone.|
18582|Trezona Formation|66202|6|Mentioned|598|||Contain primitive fossils that may be sponges. Age: Cryogenian?||||||
18582|Trezona Formation|66464|4|Described|p167, p170-174, p177|Cryogenian|Cryogenian|Adelaide Rift Complex. Intraclastic limestone breccia, stromatolite bioherms, oolitic grainstones and siltstones. Pre-glacial. Overlain by Yaltipena Formation.||||||
18582|Trezona Formation|67180|6|Mentioned|p602 Fig.2|Cryogenian|Cryogenian|Marinoan age,  Wooltana area (Preiss et al. 1998).||Unit in Umberatana Group||Overlies the Enorama Shale.||
18582|Trezona Formation|67979|6|Mentioned|p529, p530 Fig.1|Marinoan|Marinoan|Central Flinders Ranges.||Umberatana Group||||
18582|Trezona Formation|68030|6|Mentioned|p239|Cryogenian|Cryogenian|Flinders Ranges. Contains Cryogenian stromatolites.||||Overlain by Elatina Formation.||
18582|Trezona Formation|68275|6|Mentioned|p56, 58-59|||Associated with the Trezona anomaly, a large negative 13C isotope anomaly that occurred prior to the end-Cryogenian.||||Overlies Enorama Formation. Is overlain by Elatina Formation.||
18582|Trezona Formation|70031|4|Described|p245|Cryogenian|Cryogenian|Adelaide Geosyncline. Upper interglacial succession. Thickness: 240m. Records upward shallowing of the marine basin.||Unit of Upalinna Subgroup.|Includes Yaltipena Formation.|Overlain by Elatina Formation/Yerelina Subgroup, and locally by Yaltipena Formation. Underlain by Enorama Shale.|Reddish intraclastic, stromatolitic limestone and calcareous siltstone.|
18582|Trezona Formation|70082|6|Mentioned|p2|Cryogenian|Cryogenian|Flinders Ranges.||||||
18582|Trezona 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 Fortress Hill Formation.|Intraclastic and stromatolitic limestone with interbeds of calcareous siltstone.|23-JAN-19
18582|Trezona Formation|70407|5|Briefly described|p103 Fig 2, 105|Neoproterozoic|Neoproterozoic|Age: Marinoan.||Of Umberatana Group.||||
18582|Trezona Formation|71237|14|Not recorded|p10, 12, 18|||||||||
18582|Trezona Formation|72449|5|Briefly described|p1, p2 Map Legend|Neoproterozoic|Neoproterozoic|Marks return to near-shore,, tidally influenced and lagoonal environment. Shows karst topography. Shown in image on p1, 'Stromatolites in the Trezona Formation (photo 042161).||||Overlies Enorama Shale and underlies Elatina Formation.|Red and pale grey, fine-grained limestone with stromatolites and algal mud-flakes, alternating with greenish grey laminated shale and siltstone.|
18582|Trezona Formation|72473|6|Mentioned|p4|||||||||
18582|Trezona Formation|72489|4|Described|p3, p5 Fig.4, p6, p7, p10, p12|Cryogenian|Cryogenian|Adelaide Rift Complex. Non-glacial interlude. Includes stromatolites.||||Underlies Elatina Formation.|Stromatolitic bioherms, oolitic grainstone, intraclast breccia, and packstone.|
18582|Trezona Formation|73255|6|Mentioned|p534 Fig.2|Cryogenian|Cryogenian|Contains Tungussia etina stromatolite fossils.||||Overlies the Enorama Formation, underlies the Elatina Formation.||
18582|Trezona Formation|74367|5|Briefly described|p7 Fig.6, p8-9, p11, p16-17, p20, p22|Cryogenian|Cryogenian|See also p14.|674+/-11 Ma LA-ICP-MS detrital zircon MDA|Upalinna Subgroup||||
18694|Tunkalilla Formation|22581|5|Briefly described|Fig.2,p37|||Kanmantoo Group, Kanmantoo Basin. Overlies Tappanappa Formation. Overlain by Balqhidder Formation||||||
18694|Tunkalilla Formation|22643|6|Mentioned|p186|Proterozoic|Proterozoic|||||||
18694|Tunkalilla Formation|22840|6|Mentioned|Table1 P38|||||||||
18694|Tunkalilla Formation|23317|5|Briefly described|380 Fig.2|||||||||
18694|Tunkalilla Formation|23539|5|Briefly described|Fig 1 p 467|||||||||
18694|Tunkalilla Formation|23981|5|Briefly described|p13|Early Cambrian|Early Cambrian|Of the Kanmantoo Group. Geological Province: Stansbury Basin (Fleurieu Peninsula).||||||04-FEB-08
18694|Tunkalilla Formation|23996|5|Briefly described|p352 Fig.1|Cambrian|Cambrian|Of Kanmantoo Group.||||||
18694|Tunkalilla Formation|24465|4|Described|p357|Early Cambrian|Early Cambrian|Of Bollaparudda Subgroup (Kanmantoo Group).  Approx. 250m thick at type section.||||||19-JAN-05
18694|Tunkalilla Formation|30380|5|Briefly described|p198|||||||||
18694|Tunkalilla Formation|30381|3|Fully described|p216|||See also Fig.3||||||
18694|Tunkalilla Formation|35255|6|Mentioned|Fig.8|||||||||
18694|Tunkalilla Formation|36836|6|Mentioned|Table 1|||||||||
18694|Tunkalilla Formation|38873|4|Described|Table 2|||||||||
18694|Tunkalilla Formation|40442|6|Mentioned|Table 1|||||||||
18694|Tunkalilla Formation|40454|5|Briefly described|p46|||||||||
18694|Tunkalilla Formation|40455|5|Briefly described|p71|||||||||
18694|Tunkalilla Formation|41947|6|Mentioned|p16|||||||||
18694|Tunkalilla Formation|42222|6|Mentioned|Table 1 P4|||||||||
18694|Tunkalilla Formation|42225|6|Mentioned|Fig.4 P224|||||||||
18694|Tunkalilla Formation|42271|6|Mentioned|Fig.5 P376|||||||||
18694|Tunkalilla Formation|42505|5|Briefly described|Map legend|Cambrian||||||||
18694|Tunkalilla Formation|42788|5|Briefly described|Fig.14 P148|||Of Kanmantoo Group.||||||27-MAY-08
18694|Tunkalilla Formation|43703|5|Briefly described|p75|||||||||
18694|Tunkalilla Formation|43759|6|Mentioned|p445|||||||||
18694|Tunkalilla Formation|44133|4|Described|p4 Fig. 7.2, 18|Middle Cambrian|Early Cambrian|Geological Province: Stansbury Basin. Of the Kanmantoo Group. Conformably overlies: Tapanappa Formation. Maximum Thickness: 250m+||||||
18694|Tunkalilla Formation|61046|5|Briefly described|p8 Fig. 2|Early Cambrian|Early Cambrian|Of Kanmantoo Group. Carbonaceous metasiltstone, metasandstone.||||||
18694|Tunkalilla Formation|61307|5|Briefly described|p6 Fig. 3|Cambrian|Cambrian|Geological Province: Adelaide Fold Belt.||||||
18694|Tunkalilla Formation|63848|6|Mentioned|p531,  p534 Fig.4.|||Southern Fleurieu Peninsula. Possibly contains poorly preserved trilobites.||Unit in Kanmantoo Group.||Overlies Tapanappa Formation.||
18694|Tunkalilla Formation|64282|5|Briefly described|Map legend|Early Cambrian|Early Cambrian|Of the Kanmantoo Group. Geological Province: Kanmantoo Trough. Dark blue-grey, iron-stained phyllite and siltstone. Discrete beds of carbonaceous, sulphidic phyllite with pyrite moulds. Erosional base with phyllite chip conglomerate and conglomerate beds.||||||24-JUL-08
18694|Tunkalilla Formation|65375|5|Briefly described|p33.|Early Cambrian|Early Cambrian|||Unit in Kanmantoo Group.||Overlies Tapanappa Formation. Is overlain by Balquhidder Formation.||
18694|Tunkalilla Formation|65664|5|Briefly described|p1096, p1106 Fig.5|||||Of Bollaparudda Subgroup.||Overlies Tapanappa Formation. Overlain by Balquhidder Formation.||09-MAY-12
18694|Tunkalilla Formation|65892|5|Briefly described|p9 Fig.4. |Middle Cambrian|Early Cambrian|Fleurieu Peninsula.||Unit in Kanmantoo Group.||Overlies Tapanappa Formation. Is overlain by Balquhidder Formation.||
18694|Tunkalilla Formation|65921|6|Mentioned|p1, p2 (map legend).|Cambrian|Cambrian|||Of the Kanmantoo Group.||||
18694|Tunkalilla Formation|68735|6|Mentioned|p235 Fig.3|Early Cambrian|Early Cambrian|Fleurieu Peninsula.||Of the Kanmantoo Group.||||10-APR-17
18694|Tunkalilla Formation|68993|6|Mentioned|p544 Fig.1|Early Cambrian|Early Cambrian|Fleurieu Peninsula.||Of the Kanmantoo Group.||||
18694|Tunkalilla Formation|73107|5|Briefly described|Map legend.|Early Cambrian|Early Cambrian|Kanmantoo Trough.||Kanmantoo Group.|||Dark blue-grey iron-stained phyllite and siltstone. Discrete beds of carbonaceous, sulphidic phyllite with pyrite moulds. Erosional base with phyllite chip conglomerate and conglomerate beds.|
18694|Tunkalilla Formation|73188|6|Mentioned|p316|Early Cambrian|Early Cambrian|Mount Lofty Ranges.||Bollaparudda Subgroup, Kanmantoo Group|||Black shale.|
18767|Ucontitichie Granite|37326|6|Mentioned|p3|||||||||
18774|Ukaparinga Schist|31292|2|Defined|p18|Adelaidean|Adelaidean|See also P19-20||||||
18806|Umberatana Group|7931|5|Briefly described|p98|Neoproterozoic|Neoproterozoic|||||||07-FEB-11
18806|Umberatana Group|9862|5|Briefly described|Map Legend|Adelaidean|Adelaidean|||||||
18806|Umberatana Group|22510|4|Described|p36, table1p37|||Age: Sturtian to Marinoan||||||
18806|Umberatana Group|22553|6|Mentioned|p77|||part of the Adelaidean sequence||||||
18806|Umberatana Group|22631|6|Mentioned|p177, fig2 p170|Cryogenian|Cryogenian|||||||
18806|Umberatana Group|22643|6|Mentioned|p186|Proterozoic|Proterozoic|||||||
18806|Umberatana Group|22646|6|Mentioned|Fig 4 on p 102|||Adelaide Geosyncline (West). .||||||
18806|Umberatana Group|22677|5|Briefly described|p734, Fig.2 p735|Neoproterozoic|Neoproterozoic|||||||
18806|Umberatana Group|22725|6|Mentioned|p242 fig1|||||||||
18806|Umberatana Group|22772|4|Described|p63,66,Table13.1|Neoproterozoic III|Cryogenian|||||||
18806|Umberatana Group|22830|6|Mentioned|P25||Adelaidean|||||||
18806|Umberatana Group|22857|5|Briefly described|p63, Tb. 13.1 (insert p70-71)|Marinoan|Sturtian|Now included in the Heysen Supergroup and belongs to a new Pangean supercycle (Veevers, 1990). Age: 700-590Ma. See also p66.||||||
18806|Umberatana Group|22869|6|Mentioned|P37|||||||||
18806|Umberatana Group|22889|5|Briefly described|p30|Neoproterozoic|Neoproterozoic|||||||
18806|Umberatana Group|22911|6|Mentioned|37|||Geol province Adelaide Geosyncline||||||
18806|Umberatana Group|22926|5|Briefly described|37|||Geol province Adelaide Geosyncline. Underlying unit Burra Group||||||
18806|Umberatana Group|22947|6|Mentioned|p16|||Mentioned under - Adelaide Geosyncline Geodevelopments.||||||
18806|Umberatana Group|22949|5|Briefly described|p27|Neoproterozoic|Neoproterozoic|||||||
18806|Umberatana Group|23054|5|Briefly described|p14,34|||||||||
18806|Umberatana Group|23176|6|Mentioned|p12||Neoproterozoic|Adelaide Geosyncline||||||
18806|Umberatana Group|23178|6|Mentioned|Fig.1||Neoproterozoic|||||||
18806|Umberatana Group|23180|6|Mentioned|p36, Fig.1|||||||||
18806|Umberatana Group|23211|6|Mentioned|p45 Fig.1|||||||||
18806|Umberatana Group|23250|5|Briefly described|p1125 Fig.3||Cryogenian|For correlates see members.||||||
18806|Umberatana Group|23282|6|Mentioned|p54|||||||||
18806|Umberatana Group|23288|6|Mentioned|Fig.5,18|||of Adelaide Geosyncline.||||||05-APR-13
18806|Umberatana Group|23315|5|Briefly described|p344|Neoproterozoic|Neoproterozoic|Subdivided into Upper, Middle and Lower Umberatana Group.||||||07-FEB-07
18806|Umberatana Group|23351|5|Briefly described|283|Neoproterozoic|Neoproterozoic|||||||
18806|Umberatana Group|23394|5|Briefly described|Map legend|Proterozoic|Proterozoic|||||||
18806|Umberatana Group|23411|6|Mentioned|Map Legend|||||||||
18806|Umberatana Group|23412|5|Briefly described|Map Legend|Proterozoic|Proterozoic|||||||
18806|Umberatana Group|23445|5|Briefly described|p437|||||||||
18806|Umberatana Group|23478|5|Briefly described|p27|||||||||
18806|Umberatana Group|23557|5|Briefly described|p95 Fig.1|Neoproterozoic III|Cryogenian|Geological Province: Adelaide Rift Complex.||||||
18806|Umberatana Group|23719|4|Described|p26|Neoproterozoic|Adelaidean|See also page 25 table 7. Overlying unit Wilpena Group. Underlying unit Burra Group. Geological Province: Gawler Craton.||||||
18806|Umberatana Group|23806|5|Briefly described|p1122 Fig. 1|Neoproterozoic|Neoproterozoic|||||||
18806|Umberatana Group|23818|5|Briefly described|p38 Fig.10, p63|Adelaidean|Adelaidean|Max. thickness: > 20 000 ft (in the southeast).||||||
18806|Umberatana Group|23913|4|Described|p110 Fig. 2|Adelaidean|Adelaidean|Geological Province: Adelaide Geosyncline.  Overlying Unit: Wilpena Group.  Underlying Unit: Burra Group (unconformable).||||||
18806|Umberatana Group|24045|5|Briefly described|p533 Fig.2|Adelaidean|Adelaidean|||||||
18806|Umberatana Group|24175|4|Described|p12|Neoproterozoic|Neoproterozoic|Lowermost part of Heysen Supergroup.||||||
18806|Umberatana Group|24176|3|Fully described|p11, p24 Tb. 1|Adelaidean|Adelaidean|Comprises the Yudnamutana, Farina, Willochra and Yerelina Sub-Groups. Overlies the Burra Group.  Age is Marinoan. Geological Province: Mount Painter Province.||||||13-FEB-08
18806|Umberatana Group|24195|5|Briefly described|p45 Fig.3|||Geological Province: Adelaide Geosyncline||||||
18806|Umberatana Group|24261|5|Briefly described|p1047 Fig.1|Neoproterozoic|Neoproterozoic|Geological Province: Gawler Craton||||||
18806|Umberatana Group|24321|5|Briefly described|Map legend|Adelaidean|Adelaidean|Includes the Yerelina, Willochra, Farina and Yudnamutana Subgroups.||||||05-APR-13
18806|Umberatana Group|24481|5|Briefly described|p829 Fig. 9|||Overlies the Burra Group. Overlain by the Wilpena Group.||||||
18806|Umberatana Group|24484|5|Briefly described|p798 Fig.1|Neoproterozoic|Neoproterozoic|||||||
18806|Umberatana Group|24546|5|Briefly described|p2 - 3 Fig.2|Neoproterozoic|Neoproterozoic|Age: ~700-620 Ma. Geological Province: Adelaide Fold Belt.||||||16-JAN-08
18806|Umberatana Group|24586|5|Briefly described|p50 Fig. 1, p51 Fig. 2|Adelaidean|Adelaidean|Of the Heysen Supergroup. Geological Province: Adelaide Geosyncline.||||||
18806|Umberatana Group|24593|5|Briefly described|p612 Fig. 1a|||Geological Province: Mount Painter Inlier.||||||
18806|Umberatana Group|29656|4|Described|Fig.3|||||||||
18806|Umberatana Group|29697|6|Mentioned|p7|||||||||
18806|Umberatana Group|29763|6|Mentioned|p45|||||||||
18806|Umberatana Group|29778|6|Mentioned|p167|||||||||
18806|Umberatana Group|29780|4|Described|p30|||||||||
18806|Umberatana Group|29781|6|Mentioned|Fig.5|||||||||
18806|Umberatana Group|29831|5|Briefly described|p175|||||||||
18806|Umberatana Group|29834|6|Mentioned|p196|||||||||
18806|Umberatana Group|29837|4|Described|p75|||||||||
18806|Umberatana Group|29840|6|Mentioned|Fig.3|||||||||
18806|Umberatana Group|29929|6|Mentioned|Fig.1|||||||||
18806|Umberatana Group|30028|6|Mentioned|Fig.4|||||||||
18806|Umberatana Group|30051|6|Mentioned|Fig.1|||Proterozoic age.||||||
18806|Umberatana Group|30052|6|Mentioned|Fig.5|||See also Fig.6. Proterozoic age.||||||
18806|Umberatana Group|30053|6|Mentioned|Fig.1|||Proterozoic age.||||||
18806|Umberatana Group|30176|6|Mentioned|Map legend|Precambrian|Adelaidean|Sturtian - Marinoan||||||
18806|Umberatana Group|30177|4|Described|p66|||Sturtian - Marinoan age.||||||
18806|Umberatana Group|30190|6|Mentioned|Fig.1|||||||||
18806|Umberatana Group|30261|6|Mentioned|Table 1|||Sturtian - Marinoan age||||||
18806|Umberatana Group|30511|6|Mentioned|p36|||||||||
18806|Umberatana Group|30516|6|Mentioned|p64|||||||||
18806|Umberatana Group|30621|5|Briefly described|p501|||Contains 2 glaciogenic units||||||
18806|Umberatana Group|30713|6|Mentioned|p106|||||||||
18806|Umberatana Group|30798|5|Briefly described|p114|||||||||
18806|Umberatana Group|30799|6|Mentioned|p2|||Stratigraphy and terminology.||||||
18806|Umberatana Group|30801|6|Mentioned|p5|||Adelaidean. Table P5-6.||||||
18806|Umberatana Group|30802|6|Mentioned|p1|||||||||
18806|Umberatana Group|30805|6|Mentioned|p1|||||||||
18806|Umberatana Group|30807|6|Mentioned|p102|||||||||
18806|Umberatana Group|30808|6|Mentioned|Fig.2|||||||||
18806|Umberatana Group|30810|6|Mentioned|p2|||Pualco Tillite is Basal formation.||||||
18806|Umberatana Group|30917|6|Mentioned|p36|||||||||
18806|Umberatana Group|30920|6|Mentioned|Map legend|Precambrian|Precambrian|Sturtian||||||
18806|Umberatana Group|30982|6|Mentioned|p434|||||||||
18806|Umberatana Group|31022|6|Mentioned|Fig. 4|||||||||
18806|Umberatana Group|31109|6|Mentioned|p20|||See also P22, 24, 26, 28, 30.||||||
18806|Umberatana Group|31698|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
18806|Umberatana Group|31923|6|Mentioned|p8|||||||||
18806|Umberatana Group|32144|6|Mentioned|p123|||Palaeotemperature||||||
18806|Umberatana Group|32146|6|Mentioned|p346|||||||||
18806|Umberatana Group|32319|6|Mentioned|p109|||Regional geology||||||
18806|Umberatana Group|32322|6|Mentioned|p109|||||||||
18806|Umberatana Group|32364|6|Mentioned|p18|||See also Fig.2||||||
18806|Umberatana Group|32505|6|Mentioned|Table 3|||||||||
18806|Umberatana Group|32510|6|Mentioned|p106|||||||||
18806|Umberatana Group|32511|6|Mentioned|Fig.1|||||||||
18806|Umberatana Group|32547|4|Described|p60|||Sturtian||||||
18806|Umberatana Group|32635|6|Mentioned|p5|||||||||
18806|Umberatana Group|32671|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
18806|Umberatana Group|32720|6|Mentioned|p7|||Late Adelaidean||||||
18806|Umberatana Group|32721|6|Mentioned|p72|||L.Camb.||||||
18806|Umberatana Group|32722|6|Mentioned|Fig.3|||Adelaidean. Stromatolite||||||
18806|Umberatana Group|32723|6|Mentioned|p101|||See also P116||||||
18806|Umberatana Group|32724|4|Described|p509|||See also p510-532. Sturtian - Marinoan||||||22-JUN-09
18806|Umberatana Group|32726|6|Mentioned|p189|||Stromatolites||||||
18806|Umberatana Group|32954|6|Mentioned|p171|||||||||
18806|Umberatana Group|33004|6|Mentioned|PP136|||||||||
18806|Umberatana Group|33037|6|Mentioned|Fig.2|||||||||
18806|Umberatana Group|33404|5|Briefly described|p108|||Proterozoic.||||||
18806|Umberatana Group|33422|6|Mentioned|Map legend|Precambrian|Precambrian|||||||
18806|Umberatana Group|33423|4|Described|p13|||||||||
18806|Umberatana Group|33474|6|Mentioned|Fig.2|||||||||
18806|Umberatana Group|33490|6|Mentioned|p11|||Stratigraphy||||||
18806|Umberatana Group|33551|6|Mentioned|Fig.1|||Proterozoic||||||
18806|Umberatana Group|33655|6|Mentioned|p90|||||||||
18806|Umberatana Group|33691|6|Mentioned|p131|||||||||
18806|Umberatana Group|33692|6|Mentioned|Fig.2|||U.Prot.||||||
18806|Umberatana Group|33794|6|Mentioned|p7|||See also Fig.2||||||
18806|Umberatana Group|33954|6|Mentioned|p97|||See also Fig.4||||||
18806|Umberatana Group|33957|6|Mentioned|p36|||See also Fig.1||||||
18806|Umberatana Group|34175|5|Briefly described|p37|||||||||
18806|Umberatana Group|34176|6|Mentioned|p49|||Adelaidean. Units of the group described.||||||
18806|Umberatana Group|34185|6|Mentioned|p129|||||||||
18806|Umberatana Group|34202|6|Mentioned|p1056|||See also P1058. Precambrian||||||
18806|Umberatana Group|34285|6|Mentioned|p178|||||||||
18806|Umberatana Group|34287|6|Mentioned|p39|||"Sturtian"||||||
18806|Umberatana Group|34291|6|Mentioned|p11|||Adelaidean. See also PP13,17||||||
18806|Umberatana Group|34318|6|Mentioned|p86|||||||||
18806|Umberatana Group|34483|6|Mentioned|p113|||||||||
18806|Umberatana Group|34534|6|Mentioned|Fig.2.13|||||||||
18806|Umberatana Group|34535|3|Fully described|p63|||Marinoan - Sturtian. Fig.16||||||
18806|Umberatana Group|34536|6|Mentioned|Map legend|Precambrian|Adelaidean|Sturtian-Marinoan||||||
18806|Umberatana Group|34537|6|Mentioned|Fig.10|||||||||
18806|Umberatana Group|34563|6|Mentioned|p67|||Correlation and stratigraphy||||||
18806|Umberatana Group|34587|6|Mentioned|p36|||Sturtian||||||
18806|Umberatana Group|34612|6|Mentioned|p98|||||||||
18806|Umberatana Group|34766|6|Mentioned|Fig.2|||||||||
18806|Umberatana Group|34812|6|Mentioned|Table 8|||See also P4||||||
18806|Umberatana Group|34833|6|Mentioned|p76|||||||||
18806|Umberatana Group|34835|6|Mentioned|Fig.2|||||||||
18806|Umberatana Group|34836|6|Mentioned|Fig.2|||||||||
18806|Umberatana Group|34844|6|Mentioned|Fig.2|||||||||
18806|Umberatana Group|34957|6|Mentioned|p395|||||||||
18806|Umberatana Group|34985|6|Mentioned|p309|||||||||
18806|Umberatana Group|35075|6|Mentioned|Fig.2|||||||||
18806|Umberatana Group|35143|6|Mentioned|Fig.2|||||||||
18806|Umberatana Group|35158|6|Mentioned|p47|||||||||
18806|Umberatana Group|35195|6|Mentioned|Fig.2|||||||||
18806|Umberatana Group|35200|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
18806|Umberatana Group|35217|6|Mentioned|p172|||||||||
18806|Umberatana Group|35232|6|Mentioned|p5|||See also Table.1||||||
18806|Umberatana Group|35255|5|Briefly described|p9|||See also Fig.3 and P13.||||||
18806|Umberatana Group|35270|6|Mentioned|Fig.3|||||||||
18806|Umberatana Group|35327|6|Mentioned|Fig.1|||||||||
18806|Umberatana Group|35328|6|Mentioned|Fig.1|||||||||
18806|Umberatana Group|35353|6|Mentioned|Fig.2|||Regional geology||||||
18806|Umberatana Group|35543|6|Mentioned|Fig.1|||Regional bedrock geology.||||||
18806|Umberatana Group|35582|6|Mentioned|Fig.2|||||||||
18806|Umberatana Group|35586|6|Mentioned|p25|||||||||
18806|Umberatana Group|35628|6|Mentioned|p10|||||||||
18806|Umberatana Group|35675|6|Mentioned|p31|||||||||
18806|Umberatana Group|36003|5|Briefly described|p1030|||||||||
18806|Umberatana Group|36081|6|Mentioned|Fig.1|||||||||
18806|Umberatana Group|36084|6|Mentioned|Fig.2|||See also P484.||||||
18806|Umberatana Group|36126|6|Mentioned|Fig.1|||||||||
18806|Umberatana Group|36137|4|Described|p3|||||||||
18806|Umberatana Group|36212|5|Briefly described|p3|||||||||
18806|Umberatana Group|36514|6|Mentioned|p55|||||||||
18806|Umberatana Group|36623|6|Mentioned|Fig.1|||||||||
18806|Umberatana Group|36731|4|Described|p124|||||||||
18806|Umberatana Group|36733|4|Described|p47|||||||||
18806|Umberatana Group|36833|6|Mentioned|Fig.1|||||||||
18806|Umberatana Group|36837|6|Mentioned|Fig.2|||||||||
18806|Umberatana Group|36839|6|Mentioned|Fig.2|||||||||
18806|Umberatana Group|36898|6|Mentioned|p182|||||||||
18806|Umberatana Group|37015|5|Briefly described|p68|||See also Fig.2.||||||
18806|Umberatana Group|37113|6|Mentioned|Fig.1|||||||||
18806|Umberatana Group|37238|6|Mentioned|p355|||||||||
18806|Umberatana Group|37461|6|Mentioned|p332|||||||||
18806|Umberatana Group|37501|6|Mentioned|p415|||||||||
18806|Umberatana Group|37627|6|Mentioned|p181|||||||||
18806|Umberatana Group|37932|6|Mentioned|p539|||||||||
18806|Umberatana Group|38004|6|Mentioned|p82|||||||||
18806|Umberatana Group|38068|4|Described|p68|||See also Fig.4.||||||
18806|Umberatana Group|38110|6|Mentioned|p2|||||||||
18806|Umberatana Group|38157|6|Mentioned|Table 1|||||||||
18806|Umberatana Group|38243|6|Mentioned|Fig.6|||||||||
18806|Umberatana Group|38581|6|Mentioned|p252|||||||||
18806|Umberatana Group|38703|6|Mentioned|p131|||||||||
18806|Umberatana Group|38704|6|Mentioned|p133|||||||||
18806|Umberatana Group|39210|6|Mentioned|Table 3|||||||||
18806|Umberatana Group|39320|6|Mentioned|p380|||||||||
18806|Umberatana Group|39344|6|Mentioned|Map legend|Precambrian|Adelaidean|Sturtian to Marinoan||||||
18806|Umberatana Group|39348|6|Mentioned|Map legend|Precambrian|Adelaidean|Sturtian to Marinoan||||||
18806|Umberatana Group|39349|6|Mentioned|Map legend|Precambrian|Adelaidean|Marinoan to Sturtian||||||
18806|Umberatana Group|39350|6|Mentioned|Map legend|Precambrian|Precambrian|Sturtian||||||
18806|Umberatana Group|39351|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
18806|Umberatana Group|39352|6|Mentioned|Map legend|Precambrian|Adelaidean|Sturtian to Marinoan||||||
18806|Umberatana Group|39635|6|Mentioned|Fig.2|||||||||
18806|Umberatana Group|39724|6|Mentioned|Fig.6|||||||||
18806|Umberatana Group|39762|6|Mentioned|Table 1|||||||||
18806|Umberatana Group|39802|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
18806|Umberatana Group|40003|5|Briefly described|Table 2|||||||||
18806|Umberatana Group|40105|6|Mentioned|p313|||||||||
18806|Umberatana Group|40228|5|Briefly described|Fig.1|||||||||
18806|Umberatana Group|40257|6|Mentioned|p287|||||||||
18806|Umberatana Group|40294|3|Fully described|p41|||||||||
18806|Umberatana Group|40442|4|Described|p8|||||||||
18806|Umberatana Group|40448|6|Mentioned|Table 1|||||||||
18806|Umberatana Group|40456|6|Mentioned|p25|||||||||
18806|Umberatana Group|40490|6|Mentioned|Table II|||||||||
18806|Umberatana Group|40595|6|Mentioned|p92|||See also Fig.8||||||
18806|Umberatana Group|40763|6|Mentioned|p209|||||||||
18806|Umberatana Group|40852|5|Briefly described|p26|||||||||
18806|Umberatana Group|40856|5|Briefly described|p312|||||||||
18806|Umberatana Group|40906|6|Mentioned|Fig.9|||||||||
18806|Umberatana Group|40910|6|Mentioned|p11|||||||||
18806|Umberatana Group|40911|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
18806|Umberatana Group|40914|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
18806|Umberatana Group|41236|6|Mentioned|p65|||||||||
18806|Umberatana Group|41256|6|Mentioned|p7|||||||||
18806|Umberatana Group|41364|6|Mentioned|p151|||||||||
18806|Umberatana Group|41400|6|Mentioned|p27|||||||||
18806|Umberatana Group|41401|6|Mentioned|p29|||||||||
18806|Umberatana Group|41402|6|Mentioned|p42|||||||||
18806|Umberatana Group|41403|6|Mentioned|p54|||||||||
18806|Umberatana Group|41404|6|Mentioned|p73|||||||||
18806|Umberatana Group|41405|3|Fully described|p125|||||||||
18806|Umberatana Group|41429|6|Mentioned|p213|||||||||
18806|Umberatana Group|41493|6|Mentioned|Table 1|||||||||
18806|Umberatana Group|41496|5|Briefly described|Fig.1|||||||||
18806|Umberatana Group|41500|6|Mentioned|Fig.1|||||||||
18806|Umberatana Group|41526|6|Mentioned|p4|||||||||
18806|Umberatana Group|41647|6|Mentioned|p834|||||||||
18806|Umberatana Group|41703|6|Mentioned|Fig. 9|||||||||
18806|Umberatana Group|41770|6|Mentioned|p246|||||||||
18806|Umberatana Group|42028|6|Mentioned|p137|||||||||
18806|Umberatana Group|42087|5|Briefly described|p13|||||||||
18806|Umberatana Group|42088|5|Briefly described|p546|||||||||
18806|Umberatana Group|42096|6|Mentioned|p37|||||||||
18806|Umberatana Group|42098|4|Described|p53|||||||||
18806|Umberatana Group|42109|5|Briefly described|Fig.1 P19|||||||||
18806|Umberatana Group|42167|6|Mentioned|Fig.2 P115|||||||||
18806|Umberatana Group|42215|6|Mentioned|Fig.2 P448|||||||||
18806|Umberatana Group|42222|4|Described|p15|||||||||
18806|Umberatana Group|42223|6|Mentioned|Table 1 P38|||||||||
18806|Umberatana Group|42235|4|Described|p139|||See also Fig.3||||||
18806|Umberatana Group|42237|6|Mentioned|Fig.2 P86|||||||||
18806|Umberatana Group|42238|4|Described|p73|||||||||
18806|Umberatana Group|42239|6|Mentioned|p160|||||||||
18806|Umberatana Group|42240|6|Mentioned|Fig.2 P165|||||||||
18806|Umberatana Group|42243|4|Described|p211|||||||||
18806|Umberatana Group|42271|6|Mentioned|p372|||||||||
18806|Umberatana Group|42272|6|Mentioned|p402|||||||||
18806|Umberatana Group|42357|6|Mentioned|p9|||||||||
18806|Umberatana Group|42410|6|Mentioned|p3|||||||||
18806|Umberatana Group|42469|5|Briefly described|p22|||Stuart Shelf||||||
18806|Umberatana Group|42505|5|Briefly described|Map legend|Adelaidean (Marinoan)|Adelaidean (Sturtian)|||||||
18806|Umberatana Group|42542|6|Mentioned|p11|||||||||
18806|Umberatana Group|42544|5|Briefly described|Fig.1 P17|||||||||
18806|Umberatana Group|42546|5|Briefly described|Map legend|Adelaidean (Marinoan)|Adelaidean (Sturtian)|||||||
18806|Umberatana Group|42600|6|Mentioned|p6|||||||||
18806|Umberatana Group|42643|6|Mentioned|Fig. 4 P19|||||||||
18806|Umberatana Group|42720|5|Briefly described|map legend|Marinoan|Sturtian|||||||
18806|Umberatana Group|42723|5|Briefly described|map legend|Sturtian||||||||
18806|Umberatana Group|42733|5|Briefly described|map legend|Adelaidean||||||||
18806|Umberatana Group|42736|5|Briefly described|map legend|Neoproterozoic||||||||
18806|Umberatana Group|42761|5|Briefly described|Fig.2 P8|||||||||
18806|Umberatana Group|42763|5|Briefly described|Fig.2 P21|||||||||
18806|Umberatana Group|42813|4|Described|p17|||||||||
18806|Umberatana Group|42871|5|Briefly described|p90|||||||||
18806|Umberatana Group|42882|5|Briefly described|p5, Table 1 p3|||Of Heysen Supergroup.||||||03-FEB-09
18806|Umberatana Group|43052|4|Described|p183,Table 6.1|||||||||
18806|Umberatana Group|43053|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Marine and marginal marine siltstone and sandstone; oolitic, sandy and stromatolitic limestone. Glaciomarine diamictite, sandstone and siltstone and aeolian sandstone (Stuart Shelf) at top.||||||26-MAY-05
18806|Umberatana Group|43086|6|Mentioned|Appendix, Stop 7|||||||||12-JUL-16
18806|Umberatana Group|43094|6|Mentioned|p35|||||||||
18806|Umberatana Group|43190|5|Briefly described|p29, Fig.2.|||||||||
18806|Umberatana Group|43258|5|Briefly described|Map Legend||Neoproterozoic|||||||
18806|Umberatana Group|43298|5|Briefly described|Map Legend||Adelaidean|||||||
18806|Umberatana Group|43390|14|Not recorded|p3,diag.p8|||||||||
18806|Umberatana Group|43595|5|Briefly described|p545||Neoproterozoic|||||||
18806|Umberatana Group|43742|6|Mentioned|p37||Neoproterozoic|||||||
18806|Umberatana Group|43845|5|Briefly described|Fig3 p43 etc||Neoproterozoic|||||||12-JUL-16
18806|Umberatana Group|44111|6|Mentioned|p.58 Fig. 2|||in Adelaide Geosyncline||||||
18806|Umberatana Group|44133|5|Briefly described|p46, 51 Fig. 7.18|Adelaidian|Adeladian|Diamictite, siltstone, sandstone, limestone.||||||
18806|Umberatana Group|44538|4|Described|map legend|||(H53-16). Geol.Atlas Series. Equivalents: Pernatty Grit. Woocalla Dolomite Member. Sturtian.||||||
18806|Umberatana Group|44659|5|Briefly described|map legend|||Sturtian-Marinoan, lithology.||||||
18806|Umberatana Group|44660|14|Not recorded|map legend|||Marinoan, lithology.||||||
18806|Umberatana Group|44689|14|Not recorded|map legend|||Andamooka. (H53-12).||||||
18806|Umberatana Group|44690|4|Described|map legend|||Geol. Atlas Series. (I/54-5). Includes, - Grampus Quartzite, Pepuarta Tillite, Tarcowie Siltstone, Pekina Fm., Tapley Hill Fm., Braemar Iron Fm., Appila Tillite, Kadlunga Slate, Gilbert Range Quartzite, Mintaro Shale,Leasingham Quartzite.Sturtian-Marinoan||||||
18806|Umberatana Group|44934|5|Briefly described|Map Legend||Adelaidean|||||||
18806|Umberatana Group|45149|6|Mentioned|Table 1|||Page 17.||||||
18806|Umberatana Group|45155|6|Mentioned|Fig.7|||Adelaide geosyncline||||||
18806|Umberatana Group|47009|6|Mentioned|p330|||||||||
18806|Umberatana Group|47012|6|Mentioned|p332|||||||||
18806|Umberatana Group|60712|5|Briefly described|p28 Fig. 1|Adelaidean|Adelaidean|Geological Province: Adelaide Geosyncline.||||||31-MAY-05
18806|Umberatana Group|60718|4|Described|p48, p49 Fig. 1, p52, 55|Adelaidean|Adelaidean|Geological Province: Adelaide Geosyncline. See also p51 Fig. 3.|||Comprises Yudnamutana, Nepouie and Upalinna Subgroups.|Unconformably overlies Callanna or Burra Groups.||15-APR-11
18806|Umberatana Group|60953|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Includes Nepouie and Upalinna Subgroups.||||||
18806|Umberatana Group|60955|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Includes: Elatina Formation, Amberoona Formation, Tapley Hill Formation.||||||
18806|Umberatana Group|60959|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Of the Heysen Supergroup.||||||
18806|Umberatana Group|61108|5|Briefly described|map legend|Adelaidean|Adelaidean|Mainly interglacial Nepouie Subgroup and Upalinna Subgroup. Marine and marginal marine siltstone and sandstone; oolitic, sandy and stromatolitic limestone.||||||06-JUN-05
18806|Umberatana Group|61238|5|Briefly described|p44 Fig. 1|Neoproterozoic|Neoproterozoic|Includes Yudnamutana, Nepouie, Upalinna and Yerelina Subgroups.||||||10-MAY-07
18806|Umberatana Group|61307|6|Mentioned|p5|||Geological Province: Adelaide Fold Belt.||||||
18806|Umberatana Group|61308|5|Briefly described|p6|Adelaidean|Adelaidean|Limestone, siltstone and glacial deposits.||||||30-JUN-06
18806|Umberatana Group|61732|5|Briefly described|p3 Fig. 2, p4 Fig. 3|Marinoan|Sturtian|Includes subgroups: Yudnamutana, Upalinna and Yerelina; and the 657+/-17Ma Marino Arkose Member. Geological Province: Adelaide Rift Complex/Stuart Shelf.||||||05-APR-13
18806|Umberatana Group|62085|4|Described|throughout|Cryogenian|Cryogenian||||Upalinna, Nepouie, Yudnamutana Subgroups; Enorama Shale; Holowilena Ironstone; Pualco, Wilyerpa, Tapley Hill, Sunderland, Etina, Trezona, Yaltipena, Elatina Formations.|||
18806|Umberatana Group|62453|5|Briefly described|p11 Fig. 7, 12 Fig. 8|Ediacaran|Cryogenian|Geological Province: Adeliade Rift Complex/Stuart Shelf.||||||
18806|Umberatana Group|62592|5|Briefly described|p50 Table 5.1.|Marinoan|Sturtian|Adelaide Geosyncline.||Unit in Heysen Supergroup.|Includes Yudnamutana, Nepouie, Upalinna and Yerelina Subgroups.|Unconformably overlies Burra Group. Is disconformably overlain by Wilpena Group.||
18806|Umberatana Group|62664|5|Briefly described|p138 Fig.2.|Neoproterozoic|Neoproterozoic|||Unit in lower Heysen Supergroup.|Includes Yudnamutana and Willochra Subgroups and Tapley Hill Formation.|Unconformably overlies Burra Group. Is unconformably overlain by Wilpena Group.||
18806|Umberatana Group|62724|5|Briefly described|p17 Fig. 4|Sturtian|Sturtian|Includes the Yudnamutana Subgroup.||||||07-FEB-11
18806|Umberatana Group|62962|5|Briefly described|p2284 Fig. 2, p2296 Tab. 6|Adelaidean|Adelaidean|Age: 657+/-17Ma (Preiss, 2000). Geological Province: Mount Painter Province.||||||07-FEB-11
18806|Umberatana Group|63020|5|Briefly described|p973|Neoproterozoic|Neoproterozoic|||||||
18806|Umberatana Group|63102|6|Mentioned|p7|Neoproterozoic|Neoproterozoic|Geological province: Curnamona Province. unconformably overlie, or are faulted against Palaeoproterozoic rocks in the Olary Domain to the west, south, and to a limited extent, the north.||||||
18806|Umberatana Group|63458|6|Mentioned|p897 Fig.19. |Cryogenian|Cryogenian|Adelaide Geosyncline.|||Includes Yudnamutana, Farina, Yerelina, Willochra Subgroups; Tapley Hill Formation; Brighton Limestone.|Is overlain by Wilpena Group.||
18806|Umberatana Group|64319|5|Briefly described|p354, p356 Fig.2, p357 Fig.3   |Neoproterozoic|Neoproterozoic|Mis-spelt as Umberatanna on p354.||||Overlies Burra Group. Is overlain by Wilpena Group.|Limestones, quartzites and shales.|
18806|Umberatana Group|64400|6|Mentioned|p4|||Contains the Nuccaleena Dolomite and Elatina Formation. In the Adelaide Rift Complex.||||||07-FEB-11
18806|Umberatana Group|64455|5|Briefly described|p138 Fig. 1|Cryogenian|Cryogenian|Includes Elatina Formation.||||||29-JAN-09
18806|Umberatana Group|64647|5|Briefly described|p38 Fig. 1, p40|Adelaidean|Adelaidean|Overlies Burra Group. Marine sediments.||||||
18806|Umberatana Group|64724|5|Briefly described|p49 Fig. 7|Ediacaran|Cryogenian|Deposited in the Adelaide Geosyncline during (and slightly after) the Centralian 2 event (~700-635 Ma)||||||
18806|Umberatana Group|64797|5|Briefly described|p151, p153 Fig.2, p160 Fig.8.|Ediacaran|Cryogenian|See also p162 Fig.9, p163 Tb.5, p165-166. Adelaide Rift Complex. S-isotope data.|||Includes Fortress Hill Formation.|||
18806|Umberatana Group|64801|6|Mentioned|p110-113, p119|Neoproterozoic|Neoproterozoic|Adelaide Rift Complex. Interglacial shelf deposits.||Heysen Supergroup.|Yudnamutana, Yerelina Subgroups; Tapley Hill, Sunderland, Etina, Trezona, Yaltipena Formations; Enorama Shale.|Overlies Burra Group. Is overlain by Wilpena Group.||
18806|Umberatana Group|64829|5|Briefly described|p1084 Fig. 1|Neoproterozoic|Neoproterozoic|||||||07-FEB-11
18806|Umberatana Group|64846|6|Mentioned|p197 Fig.2, p198 Fig.3, p199  |Cryogenian|Cryogenian|See also p208 Fig.10, p212.|||Includes Yudnamutana, Nepouie, Upalinna and Yerelina Subgroups.|||
18806|Umberatana Group|65313|6|Mentioned|p576 Fig. 5|Neoproterozoic|Neoproterozoic|||||||
18806|Umberatana Group|65365|5|Briefly described|p10 Fig. 4|Ediacaran|Cryogenian|Adelaide Rift Complex / Stuart Shelf. Includes Marino Arkose Member.||||||
18806|Umberatana Group|65366|5|Briefly described|p23 Fig. 3|Ediacaran|Cryogenian|Adelaide Rift Complex / Stuart Shelf. Includes Marino Arkose Member.||||||
18806|Umberatana Group|65376|6|Mentioned|p92 Fig. 2.82. |Neoproterozoic|Neoproterozoic|||||||
18806|Umberatana Group|65379|6|Mentioned|p643|||Includes Tindelpina Shale Member, Tapley Hill Formation and Mount Curtis Tillite. Asbestos occurrence hosted in dolomite and/or limestones in this group.||||||07-MAR-12
18806|Umberatana Group|65483|6|Mentioned|p19|Neoproterozoic|Neoproterozoic|Underlies Tent Hill Formation (Wilpena Group).||||||28-JAN-11
18806|Umberatana Group|65493|4|Described|p907-10, 924, Fig 1,2|Cryogenian|Cryogenian|Thick interglacial succession, includes thick platform carbonate deposits. Age: U-Pb zircon 658 Ma (tuff). By correlation of the Ghaub (Nambia) and Nantuo (South China) Formations with the underlying Elatina Formation, an interval of >15 Ma is available for deposition of this sequence.||||||
18806|Umberatana Group|65892|6|Mentioned|p33 Fig.18.|Cryogenian|Cryogenian||||Includes Pualco, Wilyerpa, Tapley Hill, Sunderland, Etina, Trezona, Yaltipena and Elatina Formations; Holowilena Ironstone; Enorama Shale.|||
18806|Umberatana Group|65921|6|Mentioned|p2 (map legend)|Neoproterozoic|Neoproterozoic|||||||
18806|Umberatana Group|65925|5|Briefly described|p124 Fig.3, Appendix 2.||||||Includes Merinjina Tillite, Tapley Hill and Balcanoona Formations.||Tillite; sandstone; siltstone; arkose; dolomite; quartzite; conglomerate; shale; greywacke.|
18806|Umberatana Group|66464|5|Briefly described|p167, p168 Fig.2|Cryogenian|Tonian|Adelaide Rift Complex. Glacimarine deposits containing diamictite, sandstone, siltstone, limestone, dolomite, conglomerate and shale. 659.7 Ma. Sturtian glaciation.||||||
18806|Umberatana Group|66518|5|Briefly described|p19 Fig.4, p23.|Neoproterozoic|Neoproterozoic|Coombalarnie Platform. c.550m of this unit overlies c.700m of Burra Group in an 11 x 14 km basin west of Kalkaroo in a potential geothermal project.|||Includes Yudnamutana Subgroup.|Unconformably overlies Burra Group. Is overlain unconformably by Wilpena Group.||
18806|Umberatana Group|66884|5|Briefly described|p36-37, p41 Fig.3|||Undifferentiated. Shown also as Lower Umberatana Group in Fig.3 and lower Umberatana Group in text. Thickness: >2200 m.||Heysen Supergroup|Tindelpina Shale Member||Diamictite: well-rounded, pebble to boulder conglomerate with clasts of granite, granite porphyry, quartzite and dolostone; polymict, basal pebble conglomerate interpreted as tillite deposits; dolomite-rich siltstone interpreted as loessite deposits.|14-DEC-16
18806|Umberatana Group|67180|5|Briefly described|p599-600, p608, p612, Figs. 1, 2|Cryogenian|Cryogenian|Established by Thomson et al (1964). Poor age constraints.|||Includes Nepouie Subgroup, Upalinna Subgroup, Yudnamutana Subgroup, Yerelina Subgroup|||
18806|Umberatana Group|67484|6|Mentioned|p294 Tb.1|Cryogenian|Cryogenian|Adelaide Rift Complex.|||Includes Nuccaleena, Elatina and Tapley Hill Formations; Sturtian Tillite.|||27-MAY-15
18806|Umberatana Group|67536|6|Mentioned|Map Legend||||||||Marine siltstone and sandstone; oolitic, sandy and stromatolitic limestone; overlain and underlain by glaciomarine successions of diamictite, sandstone and siltstone.|
18806|Umberatana Group|67620|6|Mentioned|p5|Cryogenian|Cryogenian|Adelaide Rift Complex.||||Is overlain by Wilpena Group.||
18806|Umberatana Group|67870|5|Briefly described|p5, p9-10, p13, p17-18, p20-21, p23-25|Neoproterozoic|Neoproterozoic|See also p29-33. Adelaide Rift System. Thickens towards the east. Produces indistinct sets of low amplitude, discontinuous seismic reflections. The base of this unit is a major erosional surface, making an obvious sequence boundary.|||Yudnamutana, Nepouie, Upalinna, Yerelina Subgroups.|Unconformably overlies Burra Group.||
18806|Umberatana Group|67979|4|Described|p527-p531, p536, p537, p542-543, p545|Marinoan|Sturtian|Of Northern and Central Flinders Ranges. In the Adelaide Geosyncline, the initial and terminal occurrences of the Sturtian (Yudnamutana Subgroup) and Marinoan (Yerelina Subgroup) glacials define the basal and upper-most contacts of this group respectively. A thick complex interglacial succession containing abundant carbonate units separates the two glacial deposits. Placement of Sturtian-Marinoan Series boundary, and the Nepouie-Upalinna Subgroup boundary outside the Northern Flinders Ranges is difficult. Type section located in far Northern Flinders Ranges in Tindelpina-Mt Saturday region (p536 Fig.7). Geol. Prov: Adelaide Geosyncline|||base to uppermost: Yudnamutana Subgroup, Nepouie Subgroup, Upalinna Subgroup and Yerelina Subgroup.|overlies Burra Group; is overlain by Wilpena Group|complex array of sedimentary successions|
18806|Umberatana Group|68030|6|Mentioned|p236,238|||Flinders Ranges. 4.5km thick and encompasses two main phases of glacial deposition.||Unit of Heysen Supergroup.|Includes Tapley Hill Formation.|||
18806|Umberatana Group|68067|6|Mentioned|Map legend.|||||||||27-AUG-13
18806|Umberatana Group|68068|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Adelaide Geosyncline.|||Includes Yudnamutana, Nepouie and Upalinna Subgroups.|||
18806|Umberatana Group|68138|6|Mentioned|p156|Neoproterozoic|Neoproterozoic|Adelaide Rift Complex.|||Sturtian Tillite; Tapley Hill, Elatina, Nuccaleena Formations.|||
18806|Umberatana Group|68270|5|Briefly described|p683|Cryogenian|Cryogenian|Adelaide Rift Complex.|||Includes Elatina Formation, Tindelpina Shale Member, Marino Arkose Member and Sturt Tillite.|Overlain by Wilpena Group. Underlain by Burra Group.||
18806|Umberatana Group|68271|6|Mentioned|p694|||Adelaide Rift Complex.||||||
18806|Umberatana Group|68473|6|Mentioned|p531|||Adelaide Rift Complex.||||||
18806|Umberatana Group|68713|6|Mentioned|p19|||Deposited during the Sturt glaciation onto an unconformity surface.||||||
18806|Umberatana Group|69019|4|Described|p41-54, p144, p162.|Neoproterozoic|Neoproterozoic|Of Coats (1964); revised by Preiss et al. (1998). Includes tillites from Sturt and Elatina glaciations. Regional unconformity at the base.|||Includes Yudnamutana, Nepouie, Upalinna and Yerelina Subgroups.||Tillite, sandstone, siltstone, shale, arkose, dolomite, quartzite, greywacke and conglomerate.|
18806|Umberatana Group|69023|5|Briefly described|p63-72, p146-147|Neoproterozoic|Neoproterozoic|Defined by Coats (1964); revised by Preiss et al. (1998). Includes tillites from Sturtian and Marinoan glaciations.|||Includes Yudnamutana, Nepouie and Upalinna Subgroups.||Includes tillites.|
18806|Umberatana Group|69255|6|Mentioned|p771|Neoproterozoic|Neoproterozoic|||||||
18806|Umberatana Group|69666|6|Mentioned|p27 Fig.3|Neoproterozoic|Neoproterozoic|||||||
18806|Umberatana Group|69873|6|Mentioned|p82|||Adelaide Rift Complex. Included in diagram showing Cryogenian-Ediacaran stratigraphy and correlations with Tasmanian succession.||||||
18806|Umberatana Group|70013|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Interpreted as continental and marine sediments that accumulated within intra-continental rift basins.||||||
18806|Umberatana Group|70021|6|Mentioned|p97|Cryogenian|Cryogenian|Northern Flinders Ranges, Adelaide Geosyncline.||||||
18806|Umberatana Group|70031|5|Briefly described|p245|Cryogenian|Cryogenian|Adelaide Geosyncline.|||Incldues Yerelina, Upalinna, Nepouie and Yudnamutana subgroups.|Overlain disconformably to unconformably by Wilpena Group/Nuccaleena Formation.||
18806|Umberatana Group|70323|5|Briefly described|p213|Cryogenian|Cryogenian|Central Flinders Ranges, Adelaide Geosyncline.|||Includes Nepouie and Yudnamutana subgroups.|Underlain by Burra Group.||
18806|Umberatana Group|70334|5|Briefly described|p19-20,30,38,47,77,81-82,90|Neoproterozoic|Neoproterozoic|Geological province: Gawler Craton. Of Adelaide Geosyncline and Stuart Shelf. Represents the first major episode of sedimentation (basinal marine to coastal) on the Stuart Shelf during the Neoproterozoic, recording the major Sturtian and marinoan glaciation events. Underwent erosion over the Cultana Inlier during fault reactivation of the Cultana Fault.|||Includes Yerelina, Upalinna and Nepouie subgroups.|Overlain by Wilpena Group.||
18806|Umberatana Group|70384|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Adelaide Geosyncline.  Age shown more specifically as Sturtian to Marinoan [Cryogenian].||Of Heysen Supergroup.|Includes Yudnamutana, Nepouie, Upalinna, Yerelina Subgroups.|||23-JAN-19
18806|Umberatana Group|70405|6|Mentioned|p50|Neoproterozoic|Neoproterozoic|||||||
18806|Umberatana Group|70406|6|Mentioned|p121 Fig 5|||||||Overlain by Wilpena Group.||09-MAY-16
18806|Umberatana Group|70407|5|Briefly described|p102 Fig 1, p103 Fig 2, p111, 112|Neoproterozoic|Neoproterozoic|Age: Sturtian - Marinoan||Of Heysen Supergroup.|Includes Pualco Tillite,  Holowilena Ironstone, Warcowie Dolomite, Tarcowie Siltstone, Etina Formation, Enorama Shale, Trezona Formation.|||
18806|Umberatana Group|70657|5|Briefly described|p8, p54|Neoproterozoic|Neoproterozoic|Curnamona Province.||||Unconformably overlies Burra Group.|Low-grade metasedimentary rocks.|
18806|Umberatana Group|70660|6|Mentioned|p34 fig 19e|||||||||
18806|Umberatana Group|70790|6|Mentioned|p258, p260 Fig.2|Neoproterozoic|Neoproterozoic||~700-620 Ma.|||||
18806|Umberatana Group|70819|6|Mentioned|p11, 13, 29|Neoproterozoic|Neoproterozoic|Clare Valley.|||Yudnamutana, Nepouie Subgroups.|Unconformably overlies Belair Subgroup.||
18806|Umberatana Group|71037|5|Briefly described|p22-23 Fig.2, p27 Fig.6|Neoproterozoic|Neoproterozoic|Shown only on the Six Mile Hill 1:75,000 surface geology map and p27 Fig.6. Age shown as Sturtian to Marinoan.|||Includes Tapley Hill Formation, Whyalla Sandstone, Upalinna Subgroup and Yerelina Subgroup.||Sandstone, siltstone and conglomerate.|
18806|Umberatana Group|71129|4|Described|p17,21, 99, 101,107,109,111-117|Neoproterozoic|Neoproterozoic|Geological Province: Gawler Craton. Represented by basinal marine to coastal to fluvial sedimentation in SIX MILE HILL. Some outcrops and subcrops of flat-lying kaolinitic conglomerates, sandstones and shales in the Myall Creek Homestead and Myall Creek Opal Mine are tentatively assigned to the upper part of this group; these may be correlatives of the Whyalla Sandstone or the 'Yudnapinna Beds'-Wilmington Formation. Historically difficult to distinguish between Whyalla Sandstone and Yudnapinna Beds-Wilmington Formation/Upalinna Subgroup in the southwestern Stuart Shelf, and therefore sandstone successions intersected in drillholes between Tapley Hill and Tent Hill formations are variably interpreted as Whyalla sandstone or undifferentiated Umberatana Group. Maximum depositional age constrained by Re-Os age of 643+\-2.5 Ma age for the basal Tapley Hill Formation. Minimum age constrained by c. 635 Ma based on correlation of overlying Nuccaleena Formation with correlative Marinoan glacial deposits and associated cap carbonates. See also p126,134,138,184,208,225,227,.|||Includes Whyalla Sandstone, Upalinna Subgroup Yerelina Subgroup, and Nepouie Subgroup.|Overlain by Tent Hill Formation. Underlain unconformably by Broadview Schist.||13-NOV-19
18806|Umberatana Group|71130|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Age range shown as Sturtian into Marinoan.|||Upalinna and Yerelina Subgroups; Tapley Hill Formation, Whyalla Sandstone.|||
18806|Umberatana Group|71131|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Age range shown as Sturtian into Marinoan.|||Upalinna and Yerelina Subgroups; Tapley Hill Formation, Whyalla Sandstone.|||
18806|Umberatana Group|71236|6|Mentioned|p28|||||||||
18806|Umberatana Group|71237|4|Described|p7-12|||New name.||||||
18806|Umberatana Group|71238|14|Not recorded|p1,2, 10|||||||||
18806|Umberatana Group|71240|14|Not recorded|p7|||||||||
18806|Umberatana Group|71241|14|Not recorded|p13, 14, 15, p9-10|||||||||
18806|Umberatana Group|71317|6|Mentioned|p15|Neoproterozoic|Neoproterozoic|Gawler Craton.||||||
18806|Umberatana Group|71322|5|Briefly described|p52 Fig.1|Neoproterozoic|Neoproterozoic||||||Tillite, sandstone, siltstone, arkose, dolomite, quartzite, conglomerate, shale, greywacke.|
18806|Umberatana Group|71712|6|Mentioned|p411||Neoproterozoic|||||||
18806|Umberatana Group|71895|5|Briefly described|p10, p11 fig 2, p150-p151, APP4. p4, |||Stuart Shelf.|||Includes the Tapley Hill Formation, Brighton Limestone and Whyalla Sandstone.|Unconformably overlies the Beda Basalt. Overlain by the Wilpena Group.||
18806|Umberatana Group|72247|5|Briefly described|p43|Neoproterozoic|Neoproterozoic|Of Adelaide Geosyncline.||||Overlain by Wilpena Group. Underlain unconformably by Pandurra Formation.||
18806|Umberatana Group|72429|5|Briefly described|p952, p958|Sturtian|Sturtian|Mount Chambers Gorge, eastern Flinders Ranges.|||Includes the Tapley Hill Formation and the Wockerawirra Dolomite.|Underlies the Wilpena Group.|Red-brown weathered, blue-grey to green, thinly-laminated, part-flaggy siltstone and shales. Dolomitic in part.|
18806|Umberatana Group|72450|5|Briefly described|Brochure, Brochure map||||c. 650 Ma||Includes the Sturt Tillite, Tapley Hill Formation, Brighton Limestone, Angepena Formation, Marino Arkose, Wilmington Formation, Elatina Formation.|||
18806|Umberatana Group|72456|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Marree 1:250k map sheet.|||||Tillite, sandstone, siltstone, arkose, dolomite, quartzite, conglomerate, shale and greywacke.|
18806|Umberatana Group|72461|6|Mentioned|p19|Neoproterozoic|Neoproterozoic|Adelaidean Geosyncline.||||||
18806|Umberatana Group|72473|6|Mentioned|p2, p4|||Flinders Ranges, central. Brackets the Sturtian and Marinoan glaciations. The complete group is exposed within a relatively small area within the Enorama Diapir.||||||
18806|Umberatana Group|72489|6|Mentioned|p4 Fig.3|Cryogenian|Cryogenian|Adelaide Rift Complex. Only shown on p4 Fig.3. Simplified geological maps.||||||
18806|Umberatana Group|72601|6|Mentioned|p1, p5, p11, p25|Cryogenian|Cryogenian|Adelaide Rift Complex. Probably partly correlates with the Aralka Formation.||Heysen Supergroup|Tapley Hill Formation, Balcanoona Formation, Wockerawirra Dolomite, Enorama Shale, Wundowie Limestone Member, Tindelpina Shale Member|||
18806|Umberatana Group|72613|6|Mentioned|p2 fig 1, p3|Cryogenian|Cryogenian|Northern Flinders Ranges. Incorporates strata deposited during the Sturtian glaciation,  a nonglacial period between and the younger Marinoan glaciation. A tuff horizon from the uppermost Sturtian diamictite (Merinjina Diamictite/Tillite)  is dated at 663.03 +/- 0.11 Ma (Cox et al, 2018).|ca. 650 Ma||Includes the Angepena Formation, Elatina Formation, Yankaninna Formation,  Amberoona Formation, Enorama Shale, and the Weetootla Dolomite, Yudnamutana Subgroup.|||
18806|Umberatana Group|73092|6|Mentioned|p2|Cambrian|Neoproterozoic|||||||
18806|Umberatana Group|73188|5|Briefly described|p: 305, 315-316, 330, ~339-342, 351-352|Neoproterozoic|Neoproterozoic|Mount Lofty Ranges. Deposited under mainly sag-phase conditions.|||Yerelina Subgroup, Upalinna Subgroup, Nepouie Subgroup, Yudnamutana Subgroup, and units therein|||
18806|Umberatana Group|73222|5|Briefly described|p5-6, p20, p23|Cryogenian|Tonian|Adelaide Rift Complex. Sturtian to Marinoan. Thickness: 6 to 10,000 m. Deposited in glacial, glaciomarine, interglacial and post-glacial marine shelf settings. Records the Keele Peak [positive carbon isotope] excursion and the Trezona [negative carbon isotope] excursion.||Heysen Supergroup|||Diamictite, conglomerate, sandstone, and laminated siltstone.|
18806|Umberatana Group|73227|6|Mentioned|p23-25|Neoproterozoic|Neoproterozoic||||Whyalla Sandstone, Tapley Hill Formation, Elatina Formation, Brighton Limestone, Beda Basalt, Backy Point, Yudnapinna beds|||
18806|Umberatana Group|73234|6|Mentioned|p5-6, p20-21||||||Tapley Hill Formation, Brighton Limestone, Whyalla Sandstone, Yerelina Subgroup, Marino Arkose Member, Wilyerpa Formation|||
18806|Umberatana Group|73236|6|Mentioned|p35-36, p38|Ediacaran|Ediacaran|Marine sedimentary rocks.||Heysen Supergroup|Yerelina Subgroup, Upalinna Subgroup, Nepouie Subgroup, Yudnamutana Subgroup, and units therein|[Unconformably] overlain by Seacliff Sandstone (Sandison Subgroup, Wilpena Group).||
18806|Umberatana Group|73251|6|Mentioned|p36|Neoproterozoic|Neoproterozoic|Coombalarnie Platform.|||Yudnamutana Subgroup|Unconformably underlain by Burra Group. Unconformably overlain by Wilpena Group.|Metasediments.|
18806|Umberatana Group|73253|6|Mentioned|p16|||Adelaide Fold Belt. [Reworking] would contribute a zircon population centred on c. 1140 Ma coupled with zircons from age groupings 1900-1550 Ma and 2700-2100 Ma.||||||
18806|Umberatana Group|73262|6|Mentioned|p583|[Ediacaran?]|[Ediacaran?]|Includes the intervals of the Sturtian and Marinoan Glaciations.||Heysen Super Group|||Tillite, sandstone, siltstone, arkose, dolomite, quartzite, conglomerate, shale, greywacke.|
18806|Umberatana Group|74367|5|Briefly described|p3, p5-7, p15, p19, p21-22|||Thick interglacial succession up to ~4.5 km thick. Age of 713+/-38 Ma is pooled from from the Angepena Formation and Tapley Hill Formation (Webb et al., 1983) however the Tapley Hill Formation age has been confirmed as inaccurate.|713+/-38 Ma (middle part)|Heysen Supergroup|Yudnamutana Subgroup, Nepouie Subgroup, Upalinna Subgroup, Yerelina Subgroup|||
18806|Umberatana Group|75063|6|Mentioned|p94 Fig.2|||Northern Flinders Ranges area.||||||
18822|Undalya Quartzite|22889|6|Mentioned|p35|Adelaidean|Adelaidean|Parent - Bungarider Subgroup.||||||
18822|Undalya Quartzite|23818|4|Described|p60|||Geological Province: Adelaide Geosyncline. Underlying unit: Woolshed Flat Formation. Overlying unit: Auburn Dolomite. Max. thickness: ~1000 ft.||||||
18822|Undalya Quartzite|24546|5|Briefly described|p2 - 3 Fig.2|Neoproterozoic|Neoproterozoic|Of Burra Group. Overlies Mundallio Subgroup and Skillogalee Quartzite. Geological Province: Adelaide Fold Belt.||||||16-JAN-08
18822|Undalya Quartzite|29696|6|Mentioned|p2|||||||||
18822|Undalya Quartzite|29780|4|Described|p26|||||||||
18822|Undalya Quartzite|29835|6|Mentioned|p177|||||||||
18822|Undalya Quartzite|30052|6|Mentioned|Fig.5|||See also Fig.6||||||
18822|Undalya Quartzite|30782|6|Mentioned|p70|||Refers stratigraphy||||||
18822|Undalya Quartzite|30801|6|Mentioned|p5|||Table P5-6||||||
18822|Undalya Quartzite|30807|6|Mentioned|p103|||Suggested map symbol||||||
18822|Undalya Quartzite|31292|6|Mentioned|p5|||||||||
18822|Undalya Quartzite|32424|5|Briefly described|p16|||Faulting Quarries||||||
18822|Undalya Quartzite|32720|6|Mentioned|Table 1|||||||||
18822|Undalya Quartzite|32722|6|Mentioned|Fig.3|||Adelaidean. Stromatolite||||||
18822|Undalya Quartzite|32724|6|Mentioned|Fig.1|||Torrensian. Correlation||||||
18822|Undalya Quartzite|32725|6|Mentioned|p3|||Stratigraphy||||||
18822|Undalya Quartzite|33474|6|Mentioned|Fig.2|||||||||
18822|Undalya Quartzite|33951|6|Mentioned|p5|||Soil development. Formerly Stonyfell Quartzite.||||||
18822|Undalya Quartzite|33956|4|Described|p1040|||||||||
18822|Undalya Quartzite|34521|5|Briefly described|p156|||||||||
18822|Undalya Quartzite|34535|6|Mentioned|Fig.19|||Burra Gp.||||||
18822|Undalya Quartzite|34536|6|Mentioned|Map legend|Adelaidean|Adelaidean|Torrensian||||||
18822|Undalya Quartzite|34587|5|Briefly described|p36|||||||||
18822|Undalya Quartzite|34957|6|Mentioned|p395|||||||||
18822|Undalya Quartzite|35023|6|Mentioned|p132|||||||||
18822|Undalya Quartzite|35090|6|Mentioned|Fig.1|||||||||
18822|Undalya Quartzite|35255|6|Mentioned|p13|||||||||
18822|Undalya Quartzite|35270|6|Mentioned|Fig.3|||||||||
18822|Undalya Quartzite|35354|6|Mentioned|Fig.2|||Regional geology||||||
18822|Undalya Quartzite|36625|6|Mentioned|Fig.1|||||||||
18822|Undalya Quartzite|36733|6|Mentioned|Table 5|||||||||
18822|Undalya Quartzite|36834|6|Mentioned|p25|||||||||
18822|Undalya Quartzite|37461|6|Mentioned|Table 5.I|||||||||
18822|Undalya Quartzite|38157|6|Mentioned|Table III|||||||||
18822|Undalya Quartzite|38926|6|Mentioned|p34|||||||||
18822|Undalya Quartzite|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Torrensian||||||
18822|Undalya Quartzite|39352|6|Mentioned|Map legend|Adelaidean|Adelaidean|Torrensian||||||
18822|Undalya Quartzite|40294|6|Mentioned|p32|||||||||
18822|Undalya Quartzite|40501|6|Mentioned|p117|||||||||
18822|Undalya Quartzite|41404|3|Fully described|p108|||Type section described. Regional variations include laminated greenish to brownish sandy dolomite esp in Emeroo Range.|||||Well bedded medium-grained white to cream, feldspathic quartzite with interbedded  sandy carbonaceous pyritic shale|24-SEP-15
18822|Undalya Quartzite|41526|6|Mentioned|p45|||||||||
18822|Undalya Quartzite|42098|5|Briefly described|p51|||||||||
18822|Undalya Quartzite|42222|6|Mentioned|p14|||||||||
18822|Undalya Quartzite|42574|6|Mentioned|p241|||||||||
18822|Undalya Quartzite|43052|5|Briefly described|p181,Table 6.1|||||||||
18822|Undalya Quartzite|44659|5|Briefly described|map legend|||Torrensian, lithology.||||||
18822|Undalya Quartzite|44690|4|Described|map legend|||Geol. Atlas Series. (I/54-5). Unit of Burra Group. Torrensian.||||||
18822|Undalya Quartzite|62724|5|Briefly described|p17 Fig. 4|Torrensian|Torrensian|Of the Bungarider Subgroup (Burra Group).||||||07-FEB-11
18822|Undalya Quartzite|64796|6|Mentioned|p191 Fig.9|Neoproterozoic|Neoproterozoic|Appears in Fig.9 without the lithology/rank.||||Overlies Skillogalee Dolomite. Is overlain by Auburn Dolomite.||
18822|Undalya Quartzite|66522|5|Briefly described|p23.|Neoproterozoic|Neoproterozoic|Lenticular unit east of Burra; lenses out completely further east in the Nackara Arc.||Unit in Bungarider Subgroup. Occurs between Woolshed Flat Shale and Saddleworth Formation.||||
18822|Undalya Quartzite|70405|6|Mentioned|p51 table 4|Neoproterozoic|Neoproterozoic|||Bungarider Subgroup||||
18822|Undalya Quartzite|70819|5|Briefly described|p11, 13, 18, 24, 28|Neoproterozoic|Neoproterozoic|Clare Valley. Deposited in an eastward-prograding deltaic sand wedge within a marine basin. Forms a prominent ridge.||Bungarider Subgroup.||Overlies Skillogalee Dolomite. Is overlain by Watervale Sandstone.|Shallow-water, deltaic sandstones.|
18822|Undalya Quartzite|71237|14|Not recorded|p9, 18|||||||||
18822|Undalya Quartzite|71240|2|Defined|p6, p9, p18|||||||Correlated with Stonyfell Quartzite.||
18822|Undalya Quartzite|73110|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic||||||Quartzite, white to cream, medium-grained, well-bedded, feldspathic; interbeds of sandy, carbonaceous and pyritic shale.|
18822|Undalya Quartzite|73188|6|Mentioned|p340|||||||Equivalent to Stonyfell Quartzite.||
18822|Undalya Quartzite|74367|6|Mentioned|p7 Fig.6|||||Bungarider Subgroup||||
18931|Upper Middleback Jaspilite|22629|6|Mentioned|p149|Paleoproterozoic|Paleoproterozoic|part of Hutchison Group (Middleback Subgroup).||||||07-NOV-08
18931|Upper Middleback Jaspilite|23719|4|Described|p14|Paleoproterozoic|Paleoproterozoic|Also known as Mount Shannan Iron Formation. See also page 14 Table 1. Of Middleback Subgroup. O'lying unit Yadnarie Schist. U'lying unit Cook Gap Schist. Geol. Province: Gawler Craton. Max. thickness: >200 m.||||||07-NOV-08
18931|Upper Middleback Jaspilite|30806|5|Briefly described|p946|||||||||
18931|Upper Middleback Jaspilite|31034|6|Mentioned|Fig. 3|||||||||
18931|Upper Middleback Jaspilite|35298|5|Briefly described|p946|||||||||
18931|Upper Middleback Jaspilite|37811|2|Defined|p238|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
18931|Upper Middleback Jaspilite|39345|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
18931|Upper Middleback Jaspilite|39349|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
18931|Upper Middleback Jaspilite|39353|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
18931|Upper Middleback Jaspilite|41325|6|Mentioned|p15|||||||||
18931|Upper Middleback Jaspilite|41327|6|Mentioned|Fig.2|||||||||
18931|Upper Middleback Jaspilite|41619|6|Mentioned|Map legend|Paleoproterozoic||||||||07-NOV-08
18931|Upper Middleback Jaspilite|42738|5|Briefly described|map legend|Paleoproterozoic||Locally known as Mount Shannon Iron Formation.||||||07-NOV-08
18931|Upper Middleback Jaspilite|43052|5|Briefly described|p57|||of Middleback Subgroup||||||
18931|Upper Middleback Jaspilite|65376|6|Mentioned|p54. |||Name replaced by Middleback Subgroup.||||||
18931|Upper Middleback Jaspilite|65922|6|Mentioned|p15|Orosirian|Orosirian|Of Middleback Subgroup (Hutchison Group). Does not outcrop in this map area.||||||
18931|Upper Middleback Jaspilite|66302|6|Mentioned|p24|||||Hutchison Group||||
18931|Upper Middleback Jaspilite|66882|5|Briefly described|p101, p103 Fig.3a,c|||Middleback Range.||Middleback Group.||Overlies Cook Gap Schist.|Banded iron formation.|
18931|Upper Middleback Jaspilite|67536|6|Mentioned|Map Legend|||Gawler Craton.|||||Iron formation.|
18931|Upper Middleback Jaspilite|67721|5|Briefly described|p33, p33 Fig.2, p38 Fig.9|||Approximately 300 m thick.||Of the Middleback Group.|||Banded iron formation.|
18931|Upper Middleback Jaspilite|73026|5|Briefly described|p9|Paleoproterozoic|Paleoproterozoic|||||||
18931|Upper Middleback Jaspilite|73027|5|Briefly described|p9,|Palaeoproterozoic|Palaeoproterozoic||||||Amphibole-magnetite schist and quartzite.|
18976|Urana Formation|22531|5|Briefly described|p20|Permian|Carboniferous|||||||
18976|Urana Formation|22532|5|Briefly described|map legend|Permian|Carboniferous|||||||
18976|Urana Formation|22773|5|Briefly described|Fig24.5p350|Early Permian|Late Carboniferous|||||||
18976|Urana Formation|22799|2|Defined|p17|Early Permian|Late Carboniferous|||||||
18976|Urana Formation|22857|4|Described|p238, p504 App.1 Tb.A1.8|Early Permian|Late Carboniferous|Max. thickness: 900m. Geological Province: Infrabasin sediments below the Murray Basin. Correlated with Cape Jervis Formation. Geological Province: Tasman Epicratonic Province. See also p350 Fig.24.5.||||||
18976|Urana Formation|22863|6|Mentioned|p238|Early Permian|Late Carboniferous|||||||
18976|Urana Formation|22864|5|Briefly described|p259||Early Permian|||||||
18976|Urana Formation|22887|3|Fully described|p29, Fig.5 p12|Early Permian|Late Carboniferous|||||||
18976|Urana Formation|22893|2|Defined|p21 table3|Early Permian|Early Permian|Unit confined to infrabasins below Murray Basin. Fine-gr.quartzose sandstone, abundantly chloritic at top and pyritic throughout; sandstone, conglomerate, +diamictite + clasts of qtz., quartzite, black shale and pyrite traces.Cape Jervis Formation equivs.||||||22-FEB-12
18976|Urana Formation|22971|4|Described|p18, p26|Permian|Carboniferous|Entirely marine deposits - grey to black organic-rich mudstone and siltstone with marine fossils indicating Early Permian age. Max. thickness: 900m.  Present in Ovens Graben and Numurkah Trough.||||||19-JAN-06
18976|Urana Formation|23252|5|Briefly described|Map Legend||Permian|||||||
18976|Urana Formation|23309|6|Mentioned|p189||Early Permian|||||||
18976|Urana Formation|24177|4|Described|p66, p14|Permian|Late Carboniferous|Thickness may be up to 1000m. Considered the glaciomarine equivalent of Wild Duck Formation. Geological Province: Murray Basin||||||
18976|Urana Formation|24328|5|Briefly described|Map legend|Permian|Permian|||||||
18976|Urana Formation|24329|5|Briefly described|Map legend|Permian|Permian|||||||
18976|Urana Formation|24551|5|Briefly described|p212||Permian|Maximum Thickness: 887m.||||||
18976|Urana Formation|40324|2|Defined|p63|Early Permian|Late Carboniferous|Late Carboniferous to Early Permian||||||
18976|Urana Formation|41637|5|Briefly described|p208|||||||||
18976|Urana Formation|42454|5|Briefly described|p11|||Variation on Urana Formation, NSW. Late Carboniferous to Early Permian?||||||
18976|Urana Formation|42827|5|Briefly described|p209|||||||||
18976|Urana Formation|42966|3|Fully described|p58|||||||||
18976|Urana Formation|43052|5|Briefly described|Table 2.1|||||||||
18976|Urana Formation|43218|4|Described|Fig.3 p22, p26|Early Permian|Late Carboniferous|||||||
18976|Urana Formation|43627|6|Mentioned|p16|||||||||
18976|Urana Formation|43841|4|Described|7||Early Permian|Overlain unconformably by Coorabin Coal Measures. 50m thickness drilled in Ovens Valley, may be 200m.||||||27-OCT-08
18976|Urana Formation|44093|5|Briefly described|p145 App. 1|Permian|Carboniferous|See also p245 Appendix 1. Geological Province: Kanmantoo Fold Belt.||||||
18976|Urana Formation|44133|5|Briefly described|p44, 65 Fig. 8.4, 70|Permian|Carboniferous|Geological Province: Nadda Basin. Thickness: 395m.||||||
18976|Urana Formation|44188|5|Briefly described|Map Legend|Late Permian|Early Permian|Of the Millewa group. Geological province: Kanmantoo Fold Belt/Lachlan Fold Belt. Fine-grained quartzose sandstone.||||||15-MAY-08
18976|Urana Formation|44191|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|||||||
18976|Urana Formation|60529|5|Briefly described|Map Legend|Permian|Carboniferous|Marine sediments: clay and fine- to coarse-grained sand; semi-consolidated.||||||14-JUN-06
18976|Urana Formation|60591|5|Briefly described|Map Legend|Permian|Carboniferous|Unconformably overlies the Castlemaine Supergroup. Unconformably overlain by the Renmark Group and Calivil Formation. Marine deposits: clay, minor pebbles; semi-consolidated to unconsolidated||||||
18976|Urana Formation|60592|5|Briefly described|Map Legend|Permian|Carboniferous|Unconformably overlies the Castlemaine Supergroup. Unconformably overlain by the Renmark Group and Calivil Formation. Marine deposits: clay, minor pebbles; semi-consolidated to unconsolidated||||||
18976|Urana Formation|60593|5|Briefly described|Map Legend|Permian|Carboniferous|Unconformably overlies the Castlemaine Supergroup. Unconformably overlain by the Renmark Group and Calivil Formation. Marine deposits: clay, minor pebbles; semi-consolidated to unconsolidated||||||
18976|Urana Formation|60595|5|Briefly described|Map Legend|Permian|Carboniferous|Unconformably overlies the Castlemaine Supergroup. Unconformably overlain by the Renmark Group and Calivil Formation. Marine deposits: clay, minor pebbles; semi-consolidated to unconsolidated||||||
18976|Urana Formation|60596|5|Briefly described|Map Legend|Permian|Carboniferous|Unconformably overlies the Castlemaine Supergroup. Unconformably overlain by the Renmark Group and Calivil Formation. Marine deposits: clay, minor pebbles; semi-consolidated to unconsolidated.||||||27-OCT-08
18976|Urana Formation|60597|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Marine deposits: no distinctive magnetic responses||||||
18976|Urana Formation|60599|2|Defined|p76, p14|Early Permian|Carboniferous|Prev'ly Cape Jervis Beds. Three main facies: massive to lam'd siltst.+mudst; massive to parallel lam'd sst with rare pebbles + mud clasts; fine- to med.gr.diamictite.Thickness:880m in type section. Unconformable below Renmark Gp, Calivil + Shepparton Fms.||||||27-OCT-08
18976|Urana Formation|61163|6|Mentioned|p28|||Geological Province: Lachlan Fold Belt.||||||
18976|Urana Formation|61185|5|Briefly described|p53|Permian|Late Carboniferous|Do not outcrop on NAGAMBIE. Intersected in bore hole. Consists of blue, blue-grey, grey-white and mottled brown clay. No fossils recorded.||||||07-FEB-11
18976|Urana Formation|61701|5|Briefly described|Map Legend|Permian|Carboniferous|Marine sediments: clay and fine- to coarse-grained sand; semi-consolidated.||||||
18976|Urana Formation|61702|5|Briefly described|Map Legend|Permian|Carboniferous|Marine sediments: clay and fine- to coarse-grained sand; semi-consolidated.||||||
18976|Urana Formation|61703|5|Briefly described|Map Legend|Permian|Carboniferous|Marine sediments: clay and fine- to coarse-grained sand; semi-consolidated.||||||
18976|Urana Formation|66623|5|Briefly described|p231.|Permian|Permian|Ivanhoe Trough. Broadly correlated with Yanna Tank Formation, and with Cape Jervis Formation in SA.|||||Grey and laminated claystones, interbeds of fine-grained quartz sandstone and siltstone, basal tilloids and basal conglomerate.|
18976|Urana Formation|69798|5|Briefly described|p4, p11-16, p17 Fig.14, p18-19|Permian|Permian|Oaklands Basin. Early Permian. Glaciogene marine deposits in the lower part are overlain by paralic then marine deposits. Seismic profiles.|||Cocketgedong Member.|Unconformably overlies Boorhaman Conglomerate. Is overlain by Coorabin Coal Measures.||06-FEB-18
18976|Urana Formation|70125|5|Briefly described|p396-397|Permian|Permian|Oaklands Basin. 887m of glacio-marine deposits. Early Permian. Origins and ages of sediments detailed.|~290 Ma.|||Is overlain by Coorabin Coal Measures.||
18976|Urana Formation|70718|5|Briefly described|p21|Permian|Late Carboniferous|Ovens Graben. Predominatly marine sediments.||||||
18976|Urana Formation|71593|4|Described|p44, p46, p48-p49|Permian|Permian|Glacial deposits. Maximum thickness up to 370m. Preserved in the Netherby Trough. Intersected in Gunamalary 2. See also p85, p203.|||||Fluvioglacial sedimentary outwash and till deposits.|
18976|Urana Formation|73228|5|Briefly described|p50-54|Permian|Permian|Nadda Basin. Renmark Trough, Canegrass Lobe, and Paringa Embayment. Glacigene. Unconformably underlain by a sequence of Devonian clastics of the Darling Basin. At least 395 m thick, although may be thicker in the Renmark Trough. Glaciomarine to glaciolacustrine; appears to represent a proglacial to post- or non-glacial sequence. Identified in Cooltong 1, Berri North 1, Nadda 1, and Overland Corner 1 drillholes.||||Unconformably underlain by Kanmantoo Group. Overlain[?] by Pyap Member (Monash Formation).|Shale, siltstone, sandstone and diamictite with occasional conglomeratic and carbonaceous intervals; dropstones are common in the finer clastics.|
18976|Urana Formation|73229|5|Briefly described|p66-68, p70, p74|Permian|Permian|Nadda Basin. [Analysed using pXRF; see article].|||||Shale, siltstone, sandstone, diamictite and conglomerate of the glacigene.|
18976|Urana Formation|73496|6|Mentioned|Map legend|Cisuralian|Pennsylvanian|||||||
18976|Urana Formation|73497|5|Briefly described|Map legend|Permian|Permian||||||Marine to fluvial deposits beneath Renmark Group: no distinctive magnetic or radiometric responses.|
18981|Uranno Microgranite|22834|2|Defined|P39, P42||Statherian|New formation name.||||||05-MAR-08
18981|Uranno Microgranite|24197|5|Briefly described|p74 Tb. 8.1|Paleoproterozoic|Paleoproterozoic|Age: 1750-1700Ma.||||||07-FEB-11
18981|Uranno Microgranite|41667|6|Mentioned|p36|||||||||
18981|Uranno Microgranite|43052|5|Briefly described|Table 4.4|||Of Lincoln Complex.||||||05-MAR-08
18981|Uranno Microgranite|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).||||||07-NOV-08
18981|Uranno Microgranite|61070|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Moody Suite. Equigranular, fine to medium-grained grey microgranite. Locally weakly to moderately foliated. Geological Province: Gawler Craton.||||||12-JAN-10
18981|Uranno Microgranite|65376|6|Mentioned|p83. |||||Unit in Moody Suite.||||
18981|Uranno Microgranite|71862|5|Briefly described|p7, p15, p17-p18, p24, p37, p39-p41, p43|||Outcrops in the vicinity of the Uranno Homestead and west of Kapinka Falls 25km west-northwest from Tumby Bay. Well developed foliation is observed at the fault contact with the Chinmina Monzonite.||Moody Suite||Intrudes the Hutchison Group. Faulted against the Chinmina Monzonite.|Light pink to grey, fine- to medium-grained microgranite composed of porphyritic pink K-feldspar in a matrix of plagioclase, quartz and biotite.|
18983|Uratanna Formation|22646|6|Mentioned|p 102|Early Cambrian|Early Cambrian|Situated in the Adelaide Geosyncline.||||||20-JAN-09
18983|Uratanna Formation|22766|5|Briefly described|Fig.2 p561, p561|Tommotian|Tommotian|||||||
18983|Uratanna Formation|22772|5|Briefly described|Table 13.1|Early Cambrian|Early Cambrian|||||||
18983|Uratanna Formation|22857|5|Briefly described|Tb 13.1 (insert p70), p90 Fig. 14.7B|Early Cambrian|Early Cambrian|Of the Hawker Group. Age: ~545Ma. Geological Province: Arrowie Basin.||||||
18983|Uratanna Formation|22858|6|Mentioned|p92,Fig14.7bp90-1||Cambrian|||||||
18983|Uratanna Formation|22921|6|Mentioned|37|||||||||
18983|Uratanna Formation|23211|6|Mentioned|Fig.2|||Of Hawker Group.||||||20-JAN-09
18983|Uratanna Formation|23250|5|Briefly described|p1124 Fig.2||Early Cambrian|Age: Stage 1-2 of Early Cambrian.||||||
18983|Uratanna Formation|23287|6|Mentioned|Fig.2-4|||Age: Lower Cambrian. of Adelaide Geosyncline.||||||02-NOV-12
18983|Uratanna Formation|23401|6|Mentioned|p573|||||||||
18983|Uratanna Formation|23981|5|Briefly described|p8-9 Fig. 4, p10 Fig. 5|Tommotian||Overlain by Parachilna Formation. Geological Province: Arrowie Basin. See also p52 Fig. 20.||||||04-FEB-08
18983|Uratanna Formation|24176|4|Described|p15, p23 Tb. 1|Early Cambrian|Early Cambrian|Green shale, minor purple shale, orthoquartzite, feldspathic sandstone. Overlies the Pound Quartzite unconformably.  Max. thickness: 460m.  Geological Province: Mount Painter Province.||||||03-FEB-09
18983|Uratanna Formation|24465|5|Briefly described|p345 Fig.2|Early Cambrian|Early Cambrian|Geological Province: Arrowie Basin.||||||19-JAN-05
18983|Uratanna Formation|24484|5|Briefly described|p803 Fig. 3|Cambrian|Cambrian|Disconformably overlies the Rawnsley Quartzite. Overlain by the Parachilna Formation.||||||
18983|Uratanna Formation|24586|5|Briefly described|p51 Fig. 2|Early Cambrian|Early Cambrian|Of the Hawker Group (Moralana Supergroup). Geological Province: Adelaide Geosyncline.||||||
18983|Uratanna Formation|29929|6|Mentioned|p224|||||||||
18983|Uratanna Formation|30176|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
18983|Uratanna Formation|30220|6|Mentioned|Fig.13|||||||||
18983|Uratanna Formation|30374|6|Mentioned|Fig.5|||Lower Cambrian age. Correlation||||||
18983|Uratanna Formation|30375|2|Defined|p203|Early Cambrian|Early Cambrian|||||||
18983|Uratanna Formation|30801|6|Mentioned|p5|||Lower Cambrian age. Table p5-6.||||||17-MAR-22
18983|Uratanna Formation|30807|6|Mentioned|p102|||Suggested map symbol||||||
18983|Uratanna Formation|31388|6|Mentioned|Fig.2|||||||||
18983|Uratanna Formation|32724|6|Mentioned|Fig.1|||Marinoan. Correlation||||||
18983|Uratanna Formation|32776|6|Mentioned|Fig.2|||||||||
18983|Uratanna Formation|33474|6|Mentioned|Fig.3|||||||||
18983|Uratanna Formation|33734|5|Briefly described|p494|||Correlation with Lintiss Vale Fm.,NSW.||||||
18983|Uratanna Formation|34812|6|Mentioned|p137|||||||||
18983|Uratanna Formation|35255|6|Mentioned|Fig.6|||See also p37.||||||17-MAR-22
18983|Uratanna Formation|35798|6|Mentioned|p311|||||||||
18983|Uratanna Formation|35954|6|Mentioned|Fig.2|||||||||
18983|Uratanna Formation|36083|5|Briefly described|p472|||||||||
18983|Uratanna Formation|36198|6|Mentioned|Fig.I.2|||||||||
18983|Uratanna Formation|36525|6|Mentioned|Fig.4|||||||||
18983|Uratanna Formation|37627|6|Mentioned|p186|||||||||
18983|Uratanna Formation|38004|6|Mentioned|p82|||See also Table 1.||||||
18983|Uratanna Formation|38157|6|Mentioned|p265|||See also Table XI.||||||
18983|Uratanna Formation|38224|5|Briefly described|p396|||||||||
18983|Uratanna Formation|38970|6|Mentioned|p109|||||||||
18983|Uratanna Formation|39352|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
18983|Uratanna Formation|39885|6|Mentioned|p429|||||||||
18983|Uratanna Formation|40455|6|Mentioned|Fig.2|||||||||
18983|Uratanna Formation|40763|5|Briefly described|p206|||||||||
18983|Uratanna Formation|40810|5|Briefly described|p13|||||||||
18983|Uratanna Formation|40852|6|Mentioned|p32|||||||||
18983|Uratanna Formation|40856|6|Mentioned|Fig.23.6|||||||||
18983|Uratanna Formation|41401|6|Mentioned|Table 4|||||||||
18983|Uratanna Formation|41429|6|Mentioned|p242|||||||||
18983|Uratanna Formation|41526|6|Mentioned|p3|||See also p60.||||||23-JAN-19
18983|Uratanna Formation|41801|5|Briefly described|p216|||||||||
18983|Uratanna Formation|42011|5|Briefly described|p457|||||||||
18983|Uratanna Formation|42192|6|Mentioned|p10|||||||||
18983|Uratanna Formation|42222|5|Briefly described|p20|||||||||
18983|Uratanna Formation|42225|6|Mentioned|Fig.4 P224|||||||||
18983|Uratanna Formation|42240|6|Mentioned|Fig.2 P165|||||||||
18983|Uratanna Formation|42242|5|Briefly described|p200|||||||||
18983|Uratanna Formation|42272|6|Mentioned|Fig.2 P400|||||||||
18983|Uratanna Formation|42433|5|Briefly described|p178|||||||||
18983|Uratanna Formation|42440|6|Mentioned|Fig.2 P602|||||||||
18983|Uratanna Formation|42458|5|Briefly described|Fig.2 P699|||||||||
18983|Uratanna Formation|43052|5|Briefly described|Table 2.1|||||||||
18983|Uratanna Formation|43622|6|Mentioned|p38|Early Cambrian|Neoproterozoic|||||||
18983|Uratanna Formation|43781|6|Mentioned|p5|||||||||
18983|Uratanna Formation|43845|5|Briefly described|Fig3 p43||Cambrian|||||||12-JUL-16
18983|Uratanna Formation|44133|5|Briefly described|p4 Fig. 7.2, 20|Early Cambrian|Early Cambrian|Geological Province: Arrowie Basin. Disconformably overlies: Rawnsley Quartzite.||||||02-NOV-12
18983|Uratanna Formation|45155|6|Mentioned|Fig.8|||||||||
18983|Uratanna Formation|60889|4|Described|p245-50|Early Cambrian|Neoproterozoic|Outcrops over a limited area in northern Flinders Ranges. Contains small shelly fossil assemblages, and trace fossil zones. Thickness: 500 m. Comprises lowstand wedge and submarine channel deposits overlain by transgressive prodelta siltstone and highstand delta front and shoreface clastics deposited in valleys and channels cut into the Rawnsley Quartzite. Arrowie Basin.|~545 Ma.|||Overlies (unconformably) Rawnsley Quartzite (of Wilpena Group). Is overlain disconformably (erosional) by Parachilna Formation.|Predominantly carbonate sedimentation; channel deposits, shoreface clastics and prodelta siltstone.|22-SEP-17
18983|Uratanna Formation|60953|5|Briefly described|Map Legend|Cambrian|Cambrian|Geological Province: Arrowie Basin.||||||27-APR-05
18983|Uratanna Formation|61108|5|Briefly described|map legend|Cambrian|Cambrian|Marine shelf to basinal carbonate. Geological Province: Arrowie Basin.||||||
18983|Uratanna Formation|62592|5|Briefly described|p58.|Early Cambrian|Early Cambrian|Flinders Ranges.||Unit in Hawker Group.|||Basal clastics.|
18983|Uratanna Formation|63447|5|Briefly described|p962, p963 Fig.2 |Early Cambrian|Early Cambrian|||Basal Hawker Group||||
18983|Uratanna Formation|63569|6|Mentioned|p117 Fig.1|||Arrowie Basin.||||||
18983|Uratanna Formation|64455|5|Briefly described|p138 Fig. 1|Early Cambrian|Early Cambrian|Olive siltstone. Rusophycus, Didymaulichnus, Phycodes, Cochlichus and Sabellidites (shale).||||||
18983|Uratanna Formation|64460|6|Mentioned|p208|Early Cambrian|Early Cambrian|||||||
18983|Uratanna Formation|64829|5|Briefly described|p1085|Early Cambrian|Early Cambrian|Overlain by Parachilna Formation.||||||07-FEB-11
18983|Uratanna Formation|65375|5|Briefly described|p33.|Early Cambrian|Early Cambrian|||Unit in Hawker Group.||Is overlain by Parachilna Formation.||
18983|Uratanna Formation|65686|5|Briefly described|408,  p409 Fig 2, 6-7, p417, 419, 420|Early Cambrian|Ediacaran|460m thick.||||Disconformably underlies the Parachilna Formation.||07-MAY-12
18983|Uratanna Formation|65892|5|Briefly described|p7 Fig.3, p8, p9 Fig.4, p26-27.  |Early Cambrian|Early Cambrian|See also p32, p34. Arrowie Basin. 460m thick. Submarine channel deposits overlain by transgressive prodelta siltstone, and delta front and shoreface clastics. Dispute exists as to where in the Formation should be the Precambrian-Cambrian boundary. Contains acritarchs, trilobites and trace fossils.||||Disconformably overlies Rawnsley Quartzite. Is locally overlain by Parachilna Formation.||
18983|Uratanna Formation|65925|6|Mentioned|p14 Fig.2.2.|Early Cambrian|Early Cambrian|||||||
18983|Uratanna Formation|66569|5|Briefly described|p861 fig.2,|Cambrian|Cambrian|Unconformably overlies Rawnsley Quartzite.||||||
18983|Uratanna Formation|67536|5|Briefly described|Map Legend|Drumian|Ediacaran||ca. 564 +/- 61 Ma - 526 +/- 4 Ma||||Marine shelf to basinal carbonate, minor basal sandstone and tuff.|
18983|Uratanna Formation|68030|5|Briefly described|p239,243|Cambrian|Cambrian|Flinders Ranges. Shallowing upward, incision-fill succession, up to 400 m thick. Lithologically similar to that of Ediacara Member. Comprises diverse Cambrian trace fossil assemblage.||Unit of Hawker Group.||Grades upward into, and overlain by Parachilna Formation. Infills incised valleys and canyons of Rawnsley Quartzite.||
18983|Uratanna Formation|68269|6|Mentioned|p674|Cambrian|Cambrian|Adelaide Geosyncline.||||Unconformably underlain by Rawnsley Quartzite (Wilpena Group).||
18983|Uratanna Formation|68735|5|Briefly described|p233, p233 Fig.2, p235 Fig.3|Cambrian|Cambrian|Arrowie Basin. Comprises channels and deltaic sediments deposited onto the underlying Rawnsley Quartzite. Limited distribution. Contains abundant examples of the U-shaped trace fossil Diplocraterion.||||Underlain by the Rawnsley Quartzite.||10-APR-17
18983|Uratanna Formation|68993|6|Mentioned|p544 Fig.1|Early Cambrian|Early Cambrian|Arrowie Basin.||||||
18983|Uratanna Formation|69019|3|Fully described|p61, p66-69.|Early Cambrian|Early Cambrian|Informally used by Forbes (1971) and Daily (1972); defined by Daily (1973). Type section ~4 km NW of Mt Scott, adjacent to Aroona Creek. Thickness to 110 m. Formerly part of Billy Springs Formation.||Unit in Hawker Group.||Unconformably overlies Billy Springs Formation. Is overlain disconformably by Western Spur Limestone.|Basal sandy conglomeratic dolomite with stromatolites, sandy interbeds; red-brown and olive-green siltstones separated by a distinctive pale yellow dolomicrite; siltstone and limestone at top.|
18983|Uratanna Formation|69570|6|Mentioned|p421 fig 1|Cambrian|Cambrian|Arrowie Syncline, Flinder Ranges.||||||
18983|Uratanna Formation|70384|5|Briefly described|Map legend.|Early Cambrian|Early Cambrian|Arrowie Basin.|||||Red-brown siltstone with a distinctive 0.3m thick dolomicrite cap overlain by olive-green finely-laminated siltstone; basal upward-fining succession; a top 30m unit of grey, storm-bedded sandy siltstone and fine-grained limestone.|
18983|Uratanna Formation|70833|5|Briefly described|p184,200|Cambrian|Cambrian|Of Arrowie Basin. Deposited within incised canyons and valleys cut into the underlying Rawnsley Quartzite.||||Overlain disconformably by Hawker Group. Underlain unconformably by Rawnsley Quartzite.|Prodeltaic and deltaic siltstones and sandstones.|
18983|Uratanna Formation|71129|6|Mentioned|p17|||Geological Province: Gawler Craton.||||||
18983|Uratanna Formation|71317|6|Mentioned|p15|Neoproterozoic|Neoproterozoic|Gawler Craton.||||||
18983|Uratanna Formation|72456|5|Briefly described|Map Legend|Cambrian|Cambrian|Marree 1:250k map sheet.|||||Sandstone, mudclast-rich, medium-grained to pebble quartzite; siltstone and shale, green; thin mud-cracked sandstone and limestone, fossiliferous.|
18983|Uratanna Formation|73255|6|Mentioned|p534 Fig.2|early Cambrian|early Cambrian|||||Overlies the Rawnsley Quartzite, underlies the Parachilna Formation.||
18983|Uratanna Formation|75063|6|Mentioned|p94 Fig.2|||Northern Flinders Ranges area.||||||
19000|Uroonda Siltstone Member|23818|6|Mentioned|p69|||Of the Tarcowie Siltstone.||||||
19000|Uroonda Siltstone Member|29780|2|Defined|p39|Cambrian|Cambrian|||||||
19000|Uroonda Siltstone Member|30801|6|Mentioned|p5|||Marinoan. Table P5-6||||||
19000|Uroonda Siltstone Member|30807|6|Mentioned|p103|||Suggested map symbol.||||||
19000|Uroonda Siltstone Member|32146|6|Mentioned|Fig.3|||||||||
19000|Uroonda Siltstone Member|32724|6|Mentioned|Fig.1|||Marinoan. Correlation||||||
19000|Uroonda Siltstone Member|39348|6|Mentioned|Map legend|Adelaidean|Adelaidean|Marinoan||||||
19000|Uroonda Siltstone Member|40225|6|Mentioned|Map sheet|||||||||
19000|Uroonda Siltstone Member|40294|5|Briefly described|p51|||See also P15||||||
19000|Uroonda Siltstone Member|41405|3|Fully described|p176|||||||||
19000|Uroonda Siltstone Member|44659|5|Briefly described|map legend|||Marinoan, lithology.||||||
19000|Uroonda Siltstone Member|65925|5|Briefly described|Appendix 2.||||||||Siltstone, grey-green, coarse; bands of coarse quartzitic siltstone.|
19120|Village Well Formation|9862|5|Briefly described|Map Legend|Jurassic|Jurassic|Pale grey fine sandstone, siltstone and claystone with local boulder bed.||||||
19120|Village Well Formation|23394|5|Briefly described|Map legend|Cretaceous|Jurassic|||||||
19120|Village Well Formation|23818|5|Briefly described|p141 Fig.65, 146 Fig.67|Early Cretaceous|Early Cretaceous|Geological Province: Great Artesian Basin.||||||
19120|Village Well Formation|24175|5|Briefly described|p17 Fig. 3|Valanginian|Tithonian|Geological Province: Eromanga Basin.||||||
19120|Village Well Formation|24176|3|Fully described|p19, p22 Tb. 1|Late Jurassic|Late Jurassic|Sandstone and kaolinitic sandstone.  Equivalent of Algebuckina Sandstone.  Unconformably overlies Leigh Creek Coal Measures.  Max. thickness: 21m.  Geological Province: Mount Painter Province.||||||
19120|Village Well Formation|29379|6|Mentioned|Fig.11|||Refers Forbes(1966).||||||
19120|Village Well Formation|30176|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
19120|Village Well Formation|30177|6|Mentioned|p101|||||||||
19120|Village Well Formation|30804|6|Mentioned|Table 2|||||||||
19120|Village Well Formation|30807|6|Mentioned|p102|||Suggested map symbol||||||
19120|Village Well Formation|31923|6|Mentioned|p14|||||||||
19120|Village Well Formation|33165|6|Mentioned|Chart|||Correlation chart only||||||
19120|Village Well Formation|33828|6|Mentioned|Table 3|||||||||
19120|Village Well Formation|33939|5|Briefly described|p413|||Equivalent Algebuckina Sandstone.||||||
19120|Village Well Formation|34611|6|Mentioned|p143|||Correlation chart. Fig.65. Equivalent "Mooga Formation".||||||
19120|Village Well Formation|38068|5|Briefly described|p71|||||||||
19120|Village Well Formation|40926|6|Mentioned|Table 2|||||||||
19120|Village Well Formation|41085|6|Mentioned|p87|||||||||
19120|Village Well Formation|41326|6|Mentioned|p7|||||||||
19120|Village Well Formation|42899|6|Mentioned|p347|||||||||
19120|Village Well Formation|68713|6|Mentioned|p22|Cretaceous|Jurassic|Fluvial sedimentation - mostly derived from the Bopeechee Regolith.||||||
19120|Village Well Formation|69019|4|Described|p85-87.|||Of Forbes (1966). Type section is 1.2 km SSE of Village Well, where it is 5.8 m thick. Unfossiliferous; considered to be a time equivalent to Algebuckina Sandstone.||||Is overlain gradationally to disconformably by Cadna-owie Formation or Parabarana Sandstone.|Basal white quartz-pebble conglomerate; fine pale sandstone followed by brownish siltstone with minor coarse sandstone; two upper indurated sandy units that develop brown weathering rinds.|
19120|Village Well Formation|69946|5|Briefly described|p20|||Crops out adjacent to the northern Flinders Ranges. Represents the most conclusive evidence so far for marine conditions in the upper part of the Cadna-owie Formation in SA.||||Equivalent to Cadna-owie Formation.|Includes tidal bundles within cross-sets up to 1m thick.|
19120|Village Well Formation|70384|5|Briefly described|Map legend.|Cretaceous|Jurassic|Eromanga Basin - Frome Embayment.|||||White, mildly kaolinitic, basal quartz-pebble conglomerate; overlain by intermittent fine white, grey to cream sandstone (minor slump structures, cross-bedding), siltstone with minor coarse sandstone and indurated equivalents. Unfossiliferous.|18-JAN-22
19120|Village Well Formation|72456|5|Briefly described|Map Legend|Cretaceous|Jurassic|Marree 1:250k map sheet.|||||Siltstone, pale grey; sandstone, fine-grained; minor slumps and cross-beds,.|
19163|Waarre Formation|12781|6|Mentioned|p386|Late Cretaceous|Late Cretaceous|Otway Basin. Maximum thickness 204m.||Sherbrook Group.||Overlies and abuts Copa Formation. Unconformably overlies Eumeralla Formation. Is overlain unconformably by Timboon Sandstone and Flaxman Formation.||
19163|Waarre Formation|12796|5|Briefly described|p457, p456 Fig. 2|Turonian|Turonian|Of the Sherbrook Group. Geological Province: Otway Basin.||||||
19163|Waarre Formation|22470|5|Briefly described|p13 Fig. 17|Turonian|Turonian|Of Sherbrook Group.||||||
19163|Waarre Formation|22674|5|Briefly described|Fig.2 p719|Turonian|Cenomanian|||||||
19163|Waarre Formation|23818|5|Briefly described|p166, Fig.80|||Overlying unit: Flaxman Formation.||||||
19163|Waarre Formation|23916|6|Mentioned|p534|Cretaceous|Cretaceous|||||||
19163|Waarre Formation|24284|6|Mentioned|p15 Fig.2|||Otway Basin.||||||
19163|Waarre Formation|24551|6|Mentioned|p252||Late Cretaceous|Overlies the Eumeralla Formation. Maximum Thickness: 636m.||||||
19163|Waarre Formation|29856|5|Briefly described|p38|||||||||
19163|Waarre Formation|30499|6|Mentioned|p92|||Stratigraphy||||||
19163|Waarre Formation|30578|6|Mentioned|p7|||||||||
19163|Waarre Formation|30905|6|Mentioned|Table 7.4|||||||||
19163|Waarre Formation|31424|6|Mentioned|p32|||Sedimentology||||||
19163|Waarre Formation|31714|6|Mentioned|Fig. 8|||||||||
19163|Waarre Formation|32344|6|Mentioned|Fig.2|||||||||
19163|Waarre Formation|32896|6|Mentioned|Encl.7.1.|||U.Cret.||||||
19163|Waarre Formation|33936|6|Mentioned|Fig.6|||U.Cret.||||||
19163|Waarre Formation|33943|6|Mentioned|p379|||See also P383 & Fig. 20-2.||||||
19163|Waarre Formation|34063|6|Mentioned|p3|||Table. U.Cret.||||||
19163|Waarre Formation|34148|6|Mentioned|p285|||Lower Cretaceous.||||||
19163|Waarre Formation|34611|6|Mentioned|Fig.80|||Upper Cretaceous||||||
19163|Waarre Formation|36499|6|Mentioned|p36|||||||||
19163|Waarre Formation|38155|6|Mentioned|p14|||||||||
19163|Waarre Formation|40947|6|Mentioned|p4|||||||||
19163|Waarre Formation|41269|5|Briefly described|p245|||||||||
19163|Waarre Formation|41642|6|Mentioned|Table 7.12|||||||||
19163|Waarre Formation|41714|4|Described|p303|||||||||
19163|Waarre Formation|41726|5|Briefly described|p420|||See also P425||||||
19163|Waarre Formation|41769|6|Mentioned|p69|||||||||
19163|Waarre Formation|41868|4|Described|p533|||||||||
19163|Waarre Formation|41994|5|Briefly described|p6|||||||||
19163|Waarre Formation|42152|4|Described|p13|||See also P31||||||
19163|Waarre Formation|42153|5|Briefly described|p352|||See also Fig. 15||||||
19163|Waarre Formation|42599|5|Briefly described|Fig.3 P614|||||||||
19163|Waarre Formation|42827|5|Briefly described|p533|||Of Sherbrook Group.||||||14-APR-08
19163|Waarre Formation|43171|6|Mentioned|5|||||||||
19163|Waarre Formation|43208|5|Briefly described|map legend|Turonian|Cenomanian|Of Sherbrook Group.||||||
19163|Waarre Formation|43219|5|Briefly described|Fig.3,p6.||Cenomanian|Of Sherbrook Group.||||||14-APR-08
19163|Waarre Formation|43590|4|Described|p13|Turonian|Cenomanian|||||||
19163|Waarre Formation|43744|6|Mentioned|Fig.3,p3|||||||||
19163|Waarre Formation|43783|6|Mentioned|Fig14, p11||Late Cretaceous|||||||
19163|Waarre Formation|43784|6|Mentioned|Fig10, p12||Late Cretaceous|||||||
19163|Waarre Formation|43937|5|Briefly described|Map Legend|Santonian|Aptian|||||||
19163|Waarre Formation|48581|2|Defined|p35|||See also p1,12,16,28-31,34,39,40,Fig.4,Pl.1,2. (J54-12/Port Campbell).||||||
19163|Waarre Formation|48624|14|Not recorded|p1,5,7,Fig.2|||(J54-6/Benara).||||||
19163|Waarre Formation|48631|14|Not recorded|p5,7||Cretaceous|Otway Basin.||||||
19163|Waarre Formation|48911|3|Fully described|p16|||Lower - Upper Cretaceous||||||
19163|Waarre Formation|48977|6|Mentioned|Fig.5|||||||||
19163|Waarre Formation|49060|5|Briefly described|Fig.33|||||||||
19163|Waarre Formation|61016|6|Mentioned|p13|||See also Waarre formation.  Geological Province: Otway Basin.||||||20-APR-05
19163|Waarre Formation|61017|5|Briefly described|p5, p6|Turonian|Turonian|Geological Province: Otway Basin.||||||07-FEB-11
19163|Waarre Formation|61182|3|Fully described|p15-16, p31, p87-88|Turonian|Cenomanian|Of Sherbrook Gp (originally incl. in Otway Gp). Formerly known as Waarre Sandstone also. Unconformably overlies Eumeralla Fm; conformably overlain by Flaxman Fm and Belfast Mudstone. Max. thick: 180m. Geol.Province: Otway Basin. Mainly quartz sandstone.||||||
19163|Waarre Formation|61230|5|Briefly described|p319 Fig.2, pp325-326, pp337-338.    |Turonian|Turonian|Of the Otway Delta. Delta plain to shallow marine delta front conditions. TOC values vary from high to very high. Dinoflagellate diversity increases upwards.||Unit in Sherbrook Group.||Overlain by the Flaxman Formation.|Dominantly fine-medium quartz sandstone, with carbonaceous siltstone; minor coal.|
19163|Waarre Formation|61470|5|Briefly described|p27, p28 Fig. 5|Turonian|Cenomanian|Represents the main hydrocarbon play in the Port Campbell Embayment.||||||12-OCT-05
19163|Waarre Formation|61471|6|Mentioned|p34|||See also Waarre formation.  Geological Province: Otway Basin.||||||12-OCT-05
19163|Waarre Formation|61623|6|Mentioned|p449 Fig. 4|Late Cretaceous|Late Cretaceous|Of Sherbrook Group. Geological Province: Otway Basin.||||||07-APR-09
19163|Waarre Formation|61625|5|Briefly described|p475, p476 Fig. 1, p477|Late Santonian|Late Cenomanian|Of Sherbrook Group. Geological Province: Otway Basin. Heavily burrowed carbonaceous coarse-grained sandstone. Has common microplankton.||||||07-FEB-11
19163|Waarre Formation|61626|5|Briefly described|p486, p486 Fig. 2, p488 Fig. 4, p492|Late Cretaceous|Late Cretaceous|Of Sherbrook Group. Underlain by Eumeralla Formation.  Geological Province: Otway Basin.||||||07-APR-09
19163|Waarre Formation|61628|5|Briefly described|p507, p509 Fig. 3, p510, p511|Late Cretaceous|Late Cretaceous|Of Sherbrook Group. Geological Province: Otway Basin.||||||07-APR-09
19163|Waarre Formation|63124|5|Briefly described|p48 Fig. 5.1|||Introd.by McQueen (1961).Variously Waarre Fm and Waarre Sst. Here, authors revert to Waarre Sst and Copa Fm. Conformable over Copa Fm; unconformable below Flaxman Fm. Geol.Prov:Otway Basin. May correlate with Wombat Sst Mbr (Wigunda Fm) in Duntroon Basin.||||||31-JAN-08
19163|Waarre Formation|63130|5|Briefly described|p143|Late Cretaceous|Late Cretaceous|Overlies Eumeralla Formation. Geological Province: Otway Basin.||||||06-FEB-08
19163|Waarre Formation|63269|5|Briefly described|p605|Late Cretaceous|Late Cretaceous|Otway Basin. See also Waarre Sandstone (p606-607).||Sherbrook Group.||||
19163|Waarre Formation|66245|5|Briefly described|p6 Fig.5, pp61-62 Fig.C1-C2, p68 Fig.D4.|Turonian|Turonian|Shipwreck Trough. Extensive shallow marine reservoirs and coaly source rocks combine to produce an effective petroleum system, with the right burial history.||Unit in Sherbrook Group.||Is overlain by Flaxman Formation.||
19163|Waarre Formation|67061|6|Mentioned|p546 Fig.3.|Turonian|Turonian|||Unit in Sherbrook Group.||||
19163|Waarre Formation|67366|5|Briefly described|p101, pp104-109. |Turonian|Turonian|Marginal marine and lower coastal plain sandstone and mudstone. Hosts gas reserves in Halladale and Black Watch gas fields, which were discovered by amplitude versus offset (AVO) anomalies seismic interpretation.||Basal unit in Sherbrook Group.||Is overlain by Flaxman Formation.|3 units: A is a sequence of interbedded shale and lithic sandstones; B has carbonaceous siltstone and claystone with occasional thin beds of sand; C is a fine- to coarse-grained quartz-rich sandstone with excellent porosity and permeability.|
19163|Waarre Formation|67367|5|Briefly described|p131 Fig.2. |Turonian|Turonian|Hydrocarbon reservoir. Assigned to the Austral 2 petroleum sub-system. A viable source rock.||Basal unit in Sherbrook Group.||||
19163|Waarre Formation|69297|5|Briefly described|p78, p79, p83, p84, p86, p98, p115-p117|Turonian|Cenomanian|Otway and Sorell Basins. Deposited in marine, marginal marine or coastal plain environments. Major potential reservoir unit in both the Otway and Sorell Basins.||Shipwreck Supersequence||Overlies the Copa Formation. Unconformably overlies the Eumeralla Formation. Overlain by the Flaxman Formation.|Sandstones.|
19163|Waarre Formation|69651|5|Briefly described|p10, p15, p30-34, p37-39, p43-44, p50|Late Cretaceous|Late Cretaceous|Otway Basin. Turonian. Marine, marginal marine and coastal plain sediments. First hydrocarbon column intersected in the Basin (1959). The main regional reservoir in the Basin in Victoria. Sealed by Belfast Mudstone. Modelling diagrams.||Sherbrook Group.||Unconformably overlies Eumeralla Formation (Otway Group). Is overlain by Flaxman Formation.|Includes sandstones.|
19163|Waarre Formation|69879|5|Briefly described|p424|Turonian|Turonian|Otway Basin. Hydrocarbon reservoir in the Thylacine gas-condensate field. More deeply buried sediments are possibly hydrocarbon source.||||Underlies Flaxman Formation.|Fluvio-deltaic sandstone.|
19163|Waarre Formation|70077|5|Briefly described|Nelson: Fig.2; p1-2. Regional: Fig.4|Turonian|Turonian|See also Regional: p5, p7-8, p10-12. Otway Basin. Possible viable source rock. The major regional reservoir in Victorian part of the Basin. Has produced gas in 16 inshore fields in the Port Campbell area. Distal equivalents in the Nelson Sub-basin may be important petroleum reservoirs.||Sherbrook Group.||Overlies Copa or Eumeralla Formations. Is overlain by Flaxman Formation.||
19163|Waarre Formation|70078|5|Briefly described|Northern:Fig.2; p2. Regional:Fig.4; p4-6|Turonian|Turonian|Otway Basin. Equivalent sandstones in the Sorell Basin are potential reservoirs. Contains potential structural traps (high-side fault traps and faulted anticlines).||Sherbrook Group.||Overlies Copa Formation. Is overlain by Flaxman Formation.||
19163|Waarre Formation|70193|6|Mentioned|p284 Fig 2, p285 fig 3|Turonian|Turonian|Geological province: Otway Basin. Part of the Sherbrook Supersequence.||||Unconformably overlies Eumeralla Formation.||
19163|Waarre Formation|70880|6|Mentioned|p77|Turonian|Turonian|Otway Basin.||||||
19163|Waarre Formation|71266|6|Mentioned|p614 Fig.3|Late Cretaceous|Late Cretaceous|Otway Basin.||||||
19163|Waarre Formation|73357|5|Briefly described|p20, p31, p45, p47|Turonian|Turonian|Otway Basin. Correlated with Phyllocladidites mawsonii Spore-Pollen Zone, and Palaeohystrichophora infusorioides Dinocyst Zone marking a marine transgression with marginal to shallow marine facies.||Of Sherbrook Group.||Underlies Flaxman Formation.||
19163|Waarre Formation|73383|5|Briefly described|p3, p10 Tb.3.7, p11 Tb.3.9, p21-22, p68|Turonian|Cenomanian|Otway Basin. Approximately equivalent to the S5-P1 chemostratigraphic package in lower part and S5-P2 package in upper part. Higher Fe and P values and lower Si/Al values in lower part, more quartz-rich in upper part. Mudstone-dominated Package S5-P3 is only identified in Penryn-1, interpreted as uppermost part of formation. Lithologies based on geochemistry using the ChemLith classification includes argillaceous sandstone and limestone, and using the Herron classification (1988) includes quartz arenite, Fe-sand, Fe-shale, shale, wacke and lith-arenite. See also vi, p135-136, p200-201, p262-263. Waarre Formation Unit C and Waarre Formation Unit B are used on p135 and p262, and Waarre Formation Unit A on p135-136, p262-263.||Sherbrook Group||Unconformably overlies Eumeralla Formation, Otway Group, underlies Flaxman Formation|Sandstones, mudstones. Mature quartz-rich sandstone in upper part. Mudstone-dominated package in uppermost part.|
19163|Waarre Formation|73385|5|Briefly described|p5|Turonian|Cenomanian|Otway Basin.||Sherbrook Group||Overlies Eumeralla Formation, underlies Flaxman Formation.|Marginal marine and lower coastal plain sandstones, mudstones.|
19163|Waarre Formation|73386|4|Described|p4, p6, p10, Attachment A1|Turonian|Turonian|Otway Basin. First described in Bain and McQueen (1960), and Wood and Bain (1961). Type section is defined between 2494.5 m and 2675.3 m in Port Campbell-2 (Morton et al., 1994). Four sub-units previously identified, unit D originally termed Flaxman Beds and now referred to as the Flaxman Formation. Waarre Formation unit C is the primary hydrocarbon reservoir interval in the Otway Basin. Lies within the Phyllocladidites mawsonii Spore-Pollen Zone. Formation intersected primarily in the Port Campbell Embayment, Shipwreck Trough and Mussel Platform, sediments of similar age interpreted in the central and western Otway Basin are interpreted here as Warre Formation equivalent. Waarre Formation Eq. appears in multiple boreholes, Attachment A1.||Sherbrook Group||Overlies Eumeralla Formation, Otway Group, conformably underlies Flaxman Formation|Characterised by clean quartzose sandstones, conglomerates and minor siltstones and shales.|
19163|Waarre Formation|73594|5|Briefly described|p4-5, p13-16, p24-25, p27-35, p38, p66|Turonian|Cenomanian|Principal gas-bearing reservoir in the Otway Basin. Subdivided into units A, B and C (includes Ca and Cb) in the Port Campbell Embayment, not always possible to recognise these units in other places. Thickens substantially in the Shipwreck Trough. Fluvial to marginal marine environments. Diverse assemblage of marine microplankton at base interpreted to reflect flooding over a short time period (Partridge, 1997).||Sherbrook Group||Overlies Eumeralla Formation. Underlies Flaxman Formation|Transgressive sequence of sandstones, mudstones and coals. Includes a basal fine-grained lithic sandstone interbedded with mudstones and coals, overlain by carbonaceous siltstones and mudstones, fine to coarse grained quartz sandstones.|
19212|Waite Formation|9199|5|Briefly described|Map legend|||Greenish and grey siltstone and mudstone; chalcedony in upper part.||||||
19212|Waite Formation|9394|5|Briefly described|Map Legend|Pliocene|Miocene|Siltstone, claystone, limestone (commonly silicified), sandstone.||||||
19212|Waite Formation|9694|5|Briefly described|Map Legend|Early Pliocene|Late Miocene|Chalcedonic limestone, red-brown sandstone, silty sandstone, clayey sandstone and sandy claystone.||||||
19212|Waite Formation|23844|6|Mentioned|p40|Cenozoic|Cenozoic|Chalcedonic limestone, sandstone, mudstone and sandy conglomerate. Equivalent to Mount Bleechmore Granulite on ALCOOTA||||||19-NOV-08
19212|Waite Formation|29673|6|Mentioned|p360|||||||||
19212|Waite Formation|30055|6|Mentioned|p153|||||||||
19212|Waite Formation|30582|6|Mentioned|p9|||Diprotodontid remains||||||
19212|Waite Formation|30638|6|Mentioned|p232|||Upper Miocene or Lower Pliocene||||||
19212|Waite Formation|33103|6|Mentioned|p15|||||||||
19212|Waite Formation|33104|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
19212|Waite Formation|34996|6|Mentioned|p145|||||||||
19212|Waite Formation|36213|6|Mentioned|p89|||||||||
19212|Waite Formation|38371|6|Mentioned|p666|||||||||
19212|Waite Formation|39087|6|Mentioned|p16|||||||||
19212|Waite Formation|39610|4|Described|p8|||||||||
19212|Waite Formation|39898|5|Briefly described|Map legend|Tertiary|Tertiary|Greenish-grey siltstone, chalcedony and limestone.||||||14-FEB-06
19212|Waite Formation|40538|5|Briefly described|Map legend|early Pliocene|late Miocene|Chalcedonic limestone, grey; rare sandy mudstone.||||||15-NOV-05
19212|Waite Formation|40906|6|Mentioned|p30|||||||||
19212|Waite Formation|41537|6|Mentioned|Fig.2|||||||||
19212|Waite Formation|42375|5|Briefly described|Table 1 P11|||In the Waite Basin.||||||14-DEC-06
19212|Waite Formation|42420|6|Mentioned|p256|late Miocene||||||||
19212|Waite Formation|42457|6|Mentioned|p171|||||||||
19212|Waite Formation|42504|6|Mentioned|Table 1 P4|||||||||
19212|Waite Formation|42562|6|Mentioned|p95|||||||||
19212|Waite Formation|42776|5|Briefly described|p299|||||||||
19212|Waite Formation|43225|5|Briefly described|Map Legend||Tertiary|||||||
19212|Waite Formation|43503|5|Briefly described|45|||||||||
19212|Waite Formation|43565|3|Fully described|p422,431-440|Early Pliocene|Late Miocene|||||||
19212|Waite Formation|43748|4|Described|p8,19, Tb 1, p11,15,17|Early Pliocene|Late Miocene|Waite Basin. Includes vertebrate fossil assemblage. Middle unit within informal 'Alcoota beds' succession. 40m crops out. Full thickness not known. Interbedded chalcedonic, calcarenitic limestone, sandstone, siltstone and minor sandy conglomerate.|||||Interbedded chalcedonic, calcarenitic limestone, sandstone, siltstone and minor sandy conglomerate.|19-DEC-11
19212|Waite Formation|44133|5|Briefly described|p190 Fig. 10.30|Early Pliocene|Late Miocene|Geological Province: Waite Basin.||||||
19212|Waite Formation|44223|14|Not recorded|Fig.2|||Correlation of fauna.||||||
19212|Waite Formation|44227|14|Not recorded|p.59,74,91|Early Pliocene|Late Miocene|Alcoota fauna in early Pliocene or late Miocene. Diprotodontids. (F53-10).||||||
19212|Waite Formation|44238|14|Not recorded|Fig.3|Pliocene|Miocene|||||||
19212|Waite Formation|45028|2|Defined|p10-12|Pliocene|Miocene|See also Fig.2,4, p1,8,13-17,22,45,108,125,139,149,161,162,175,176,187. late Miocene or early Pliocene. (F53-10).||||||
19212|Waite Formation|45041|5|Briefly described|p118|||Mid Tertiary||||||
19212|Waite Formation|45128|6|Mentioned|p40|||||||||
19212|Waite Formation|46800|6|Mentioned|p109|||||||||
19212|Waite Formation|60547|5|Briefly described|Map Legend|Tertiary|Tertiary|Greenish and grey siltstone and mudstone; chalcedony in upper part.||||||
19212|Waite Formation|60551|5|Briefly described|Map Legend|Pliocene|Miocene|Geological Province: Waite Basin. Chalcedonic limestone.||||||
19212|Waite Formation|60668|5|Briefly described|Fig. 22a|||Chalcedonic limestone, sandstone, mudstone and conglomerate.||||||
19212|Waite Formation|60703|5|Briefly described|p704 Fig. 2, p725 Fig.18|Pliocene|Late Miocene|Geological Province: Waite Basin.||||||12-APR-05
19212|Waite Formation|61155|5|Briefly described|p5, p16|Late Miocene|Early Miocene|Lacustrine siltstones and chalcedonic limestones of central Australia. Age: >10Ma. Thickness: 20m. Geological Province: Hale, Ti-Tree and Waite  Basins.||||||07-OCT-15
19212|Waite Formation|61388|5|Briefly described|Map Legend|Cenozoic|Cenozoic|Chalcedonic limestone, massive chalcedony.||||||19-NOV-08
19212|Waite Formation|61404|5|Briefly described|Map legend|Neogene|Paleogene|Limestone: chalcedonic; rare quartzic mudstone. Geological Province: southern Georgina Basin.||||||07-NOV-08
19212|Waite Formation|62082|5|Briefly described|p19, p52|Pliocene|Miocene|Forms caps on mesas where it is equivalent to Austral Downs Limestone and chert; often associated with duricrust. See also p53.||||||07-FEB-11
19212|Waite Formation|64068|3|Fully described|p80, 79, p42, p19|Pliocene|Miocene|Gastropods and vertebrates fossils. Overlies Cenozoic ferricrete. Is overlain by Quaternary alluvium. Lower part correlated with Poodyea Formation. Correlations: Austral Downs Limestone, Brunette Limestone, Arltunga beds.|||||Lacustrine green siltstone below fluviatile red siltstone, sandstone and conglomeratic sandstone, capped by pedogenic chalcedonic limestone.|04-APR-12
19212|Waite Formation|65194|5|Briefly described|p53, p71-72, p74|Early Pliocene|Late Miocene|Waite Basin. Equivalents occur in Ti-Tree Basin which coarsen upwards, representing a change from lacustrine to fluvial conditions; overlain by undifferentiated Cenozoic alluvial sediments.||||||08-APR-16
19212|Waite Formation|65341|5|Briefly described|p2 Fig.2, p5, p19.|Cenozoic|Cenozoic|Waite Basin. Lacustrine and fluvial deposition. Outcrops as isolated low hills and in palaeochannels. Locally contains a gastropod and vertebrate fossil fauna indicating Late Miocene or Early Pliocene age.|||||Chalcedony, chalcedonic limestone, overlying lacustrine siltstone, fluviatile siltstone, sandstone and conglomerate.|
19212|Waite Formation|66131|6|Mentioned|p242 Fig.2|Miocene|Miocene|Middle to Late Miocene in age (from Fig.2 - stratigraphic correlation chart).||||||
19212|Waite Formation|69458|5|Briefly described|p42:7-13|||Waite Basin. Forms the hard resistant summit caps of many low plateaux and mesas. From lacustrine to fluvial deposits. Contains vertebrate fossils at the Alcoota fossil site (described).||Alcoota beds.||Unconformably overlies Tug Sandstone Member (Hale Formation).|Lacustrine green-grey siltstone, followed by fluvial red siltstone, sandstone and conglomeratic sandstone, capped by pedogenic cream or white, chalcedonic calcarenitic limestone.|12-JUL-16
19212|Waite Formation|72515|5|Briefly described|Map Legend|Cenozoic|Cenozoic|Jervois Range Special Map Sheet. Waite Basin.||Alcoota beds|||Calcedonic limestone, calcite veins.|05-JUL-22
19212|Waite Formation|72516|3|Fully described|p11, p98|Pliocene|Miocene|Waite Basin. Type section occurs 6km south of Alcoota homestead. Intersected in drillhole BMR Alcoota 3. Outcrops as low plateaus and mesas peripheral to the margins of the Waite Basin on ALCOOTA and ALICE SPRINGS map sheets; equivalents are interpreted on HUCKITTA. Maximum thickness is >3m in the mapped area, 19-130m elsewhere. Deposited in a lacustrine or fluvial environment. Hosts late Miocene to early Pliocene verterbrate fossils. Interpreted to be an age correlative of the Austral Downs Limestone, Brunette Limestone and the Arltunga beds. Equivalents are interpreted in southern Huckitta.||Alcoota beds||Unconformably overlies the Denara Orthogneiss.|Chalcedonic limestone, calcite veins; recessive, lacustrine, green siltstone. Fluvial red silstone, sandstone, conglomeratic sandstone.|09-JUN-21
19226|Waldeila Formation|22525|6|Mentioned|p37.41||Holocene|scale problems for inclusion in this paper||||||
19226|Waldeila Formation|39351|6|Mentioned|Map legend|Quaternary|Quaternary|||||||
19226|Waldeila Formation|39522|6|Mentioned|p92|||||||||
19226|Waldeila Formation|44198|2|Defined|p49|Holocene|Holocene|||||||
19226|Waldeila Formation|44199|2|Defined|p594, 596, 597|Quaternary|Neogene|late Tertiary - Quaternary. Alluvial.||||||
19226|Waldeila Formation|65901|4|Described|p175-8, p180 Tab.2, p183-5|Holocene|Holocene|Forms present-day floodplains and low river terraces. Mid-Holocene age from radiocarbon and amino acid racemisation dating. Optically stimulated luminescence date of 3.5+/-0.3 ka||||Interfingers with St Kilda Formation.|Grey/black alluvium.|08-MAR-12
19319|Walloway carbonatite|40811|4|Described|p321|||||||||
19323|Wallumbilla Formation|9528|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Dark purplish grey to white, fine to medium lithic sandstone, feldspathic sandstone.||||||
19323|Wallumbilla Formation|12597|4|Described|p492 Tb.1, p497, p498, p499-500|Albian|Aptian|Eromanga Basin. Division into the two Members is not possible in the NW, where the sequence is more uniform.|||Includes Doncaster and Coreena Members.||Marine, largely argillaceous sequence with common mollusc, gastropod, scaphopod and belemnites fossils.|
19323|Wallumbilla Formation|13497|5|Briefly described|p115 fig 6.33, p138 fig 8.17|Early Cretaceous|Early Cretaceous|Eromanga Basin. See also p144 fig 9.2, p145, p146, p148-p151.||Marree Subgroup||Overlies the Cadna-owie Formation. Overlain by the Toolebuc Formation.||
19323|Wallumbilla Formation|13516|5|Briefly described|p167 fig 10, p169 fig 11, p171 fig 12|Early Cretaceous|Early Cretaceous|In Eromanga Basin.|||Includes Doncaster and Coreena Members|||
19323|Wallumbilla Formation|22464|5|Briefly described|p9||Early Cretaceous|Eromanga Basin. Overlain by Toolebuc Formation.||||||18-DEC-06
19323|Wallumbilla Formation|22744|5|Briefly described|Fig1, P12, Table4||Cretaceous|||||||
19323|Wallumbilla Formation|22747|6|Mentioned|p15||Mesozoic|||||||
19323|Wallumbilla Formation|22757|6|Mentioned|Table6,p11||Early Cretaceous|In the Surat Basin.||||||18-DEC-06
19323|Wallumbilla Formation|22857|4|Described|p296-7 Tb.22.1, p544 App.1 Tb.A1.12|Albian|Aptian|Of the Rolling Downs Group. Sequence of mudstone and siltstone. Contains the Coreena Member. Max. thickness: 600m. Geological Province: Surat and Eromanga Basins. See also p312-3 Fig. 22.6, p314-5, p544 App.1 Tb.A1.12.||||||
19323|Wallumbilla Formation|22865|4|Described|p314,Table22.1p296-7|Albian|Aptian|||||||
19323|Wallumbilla Formation|22883|5|Briefly described|P31, Fig2||Early Cretaceous|Overlying unit is Toolebuc Formation, underlying unit is Cadna-owie Formation||||||
19323|Wallumbilla Formation|22912|5|Briefly described|33|||Geological province: Eromanga Basin.||||||18-DEC-06
19323|Wallumbilla Formation|23031|5|Briefly described|31|||||||||
19323|Wallumbilla Formation|23050|5|Briefly described|p 82 Fig.17|Early Cretaceous|Early Cretaceous|Of Surat Basin.||||||18-DEC-06
19323|Wallumbilla Formation|23056|6|Mentioned|9|||Geol Province Eromanga Basin||||||
19323|Wallumbilla Formation|23065|5|Briefly described|18|||Geological  province: Carpentaria Basin. Of the Rolling Downs Group.||||||18-DEC-06
19323|Wallumbilla Formation|23071|6|Mentioned|p761|||||||||
19323|Wallumbilla Formation|23154|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|Geological Province - Eromanga Basin.  Of the Marree Subgroup (Neales River Group).||||||18-DEC-06
19323|Wallumbilla Formation|23155|4|Described|p32|Early Cretaceous|Early Cretaceous|The unit is laterally equivalent to the Bulldog Shale and it is limited to the northern part of STRZELECKI.  Age Aptian-Albian.||||||
19323|Wallumbilla Formation|23183|6|Mentioned|p222||Aptian|||||||
19323|Wallumbilla Formation|23220|5|Briefly described|p16||Mesozoic|Of the Rolling Downs Group.||||||18-DEC-06
19323|Wallumbilla Formation|23224|5|Briefly described|p3|||Hosts the Doncaster Member which hosts the Opal Deposits. Of Rolling Downs Group. In the Great Australian Basin.||||||01-FEB-07
19323|Wallumbilla Formation|23291|4|Described|p80 Tb. 3.6|Early Cretaceous|Early Cretaceous|Age: early Cretaceous. Conformably overlies Coffin Hill Member. Geological Province: Georgetown Region.||||||08-JUL-15
19323|Wallumbilla Formation|23375|4|Described|Fig2 p265|Albian|Barremian|Laterally equivalent to Bulldog Shale. of Eromanga Basin.||||||
19323|Wallumbilla Formation|23393|5|Briefly described|p24|Early Cretaceous|Early Cretaceous|Of Rolling Downs Group.||||||
19323|Wallumbilla Formation|23425|4|Described|Table 9.7 p394|Aptian|Aptian|+ Plate 9.2 + p378. Of Rolling Downs Group. Conformably overlain by Toolebuc Formation; underlain by Gilbert River Formation. Geological Province Carpentaria Basin. Max. thickness 500 m.||||||18-DEC-06
19323|Wallumbilla Formation|23430|5|Briefly described|p455|||Eromanga Basin Province.||||||
19323|Wallumbilla Formation|23496|5|Briefly described|Table 4, p59|Albian|Aptian|of Rolling Downs Group. Previously Blackdown Formation (Laing and Power 1959), then Wilgunya Subgroup (Grimes & Whittaker 1977) then of Smart and Others 1972/1980.||||||01-FEB-07
19323|Wallumbilla Formation|23499|5|Briefly described|map legend|Early Cretaceous|Early Cretaceous|In the Eromanga Basin.||||||18-DEC-06
19323|Wallumbilla Formation|23510|5|Briefly described|Map Legend||Early Cretaceous|Of the Rolling Downs Group.||||||18-DEC-06
19323|Wallumbilla Formation|23518|5|Briefly described|p13|Mesozoic|Mesozoic|Of Rolling Downs Group.  Geological Province: Carpentaria Basin.||||||
19323|Wallumbilla Formation|23713|6|Mentioned|p39|||||||||
19323|Wallumbilla Formation|23818|6|Mentioned|p141 Fig.65|||Geological Province: Great Artesian Basin. Of the Wilunga Sub-Group.||||||
19323|Wallumbilla Formation|23883|5|Briefly described|p129 Fig. 11.2|Cretaceous|Cretaceous|Of Rolling Downs Group.  Contains the Coreena and Doncaster Members.  Geological Province: Great Australian Superbasin.||||||
19323|Wallumbilla Formation|23911|5|Briefly described|p90 Fig. 4|Cretaceous|Cretaceous|Geological Province: Eromanga Basin.  Of the Rolling Downs Group.||||||
19323|Wallumbilla Formation|23982|5|Briefly described|p35 Fig.7|Cretaceous|Cretaceous|Includes the Coreena and Doncaster Members. Geological Province: Great Artesian Basin.||||||
19323|Wallumbilla Formation|23986|5|Briefly described|p71|||||||||
19323|Wallumbilla Formation|24048|5|Briefly described|p76|||||||||
19323|Wallumbilla Formation|24068|4|Described|p270 Table 2|Early Cretaceous|Early Cretaceous|Geological Province: Surat Basin.  Maximum thickness: 310m.||||||
19323|Wallumbilla Formation|24073|5|Briefly described|p378 Table 2|Early Cretaceous|Early Cretaceous|Supersedes Balckdown Formation.  Of Rolling Downs Group. Maximum thickness: 200m.  Geological Province: Carpentaria Basin.||||||
19323|Wallumbilla Formation|24085|5|Briefly described|Not recorded|Albian|Aptian|Contains Doncaster Member. Geological Province: Eromanga Basin||||||16-MAR-05
19323|Wallumbilla Formation|24092|5|Briefly described|p5|Cretaceous|Jurassic|Geological Province: Great Artesian Basin.||||||
19323|Wallumbilla Formation|24175|5|Briefly described|p17 Fig. 3|Albian|Aptian|Geological Province: Eromanga Basin.||||||
19323|Wallumbilla Formation|24204|5|Briefly described|p263 Fig.4, p267, p282 Fig.21|Early Cretaceous|Early Cretaceous|Geological Province: Eromanga Basin.||||||
19323|Wallumbilla Formation|24210|5|Briefly described|p133 Fig. 2|Early Cretaceous|Early Cretaceous|Of the Marree Subgroup?  Geological Province: Eromanga Basin.||||||
19323|Wallumbilla Formation|24243|5|Briefly described|p3 Fig.2|Cretaceous|Cretaceous|Of Rolling Downs Group.||||||
19323|Wallumbilla Formation|24251|5|Briefly described|p234 Fig.1, p245|Albian|Albian|Overlying Unit: Toolebuc Formation. Geological Province: Eromanga Basin||||||
19323|Wallumbilla Formation|29387|6|Mentioned|Table 5|||||||||
19323|Wallumbilla Formation|29393|6|Mentioned|Table 4|||Cretaceous.||||||
19323|Wallumbilla Formation|29591|6|Mentioned|p71|||||||||
19323|Wallumbilla Formation|29651|6|Mentioned|p25|||||||||
19323|Wallumbilla Formation|29721|6|Mentioned|Table 246|||||||||
19323|Wallumbilla Formation|30019|6|Mentioned|p2|||||||||
19323|Wallumbilla Formation|30020|4|Described|p29|||||||||
19323|Wallumbilla Formation|30021|6|Mentioned|p89|||||||||
19323|Wallumbilla Formation|30022|6|Mentioned|p32|||||||||
19323|Wallumbilla Formation|30024|6|Mentioned|p331|||||||||
19323|Wallumbilla Formation|30042|4|Described|p4|||? glauconite.||||||
19323|Wallumbilla Formation|30095|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|30102|6|Mentioned|Table 4|Cretaceous|Jurassic|See also P17.||||||
19323|Wallumbilla Formation|30103|5|Briefly described|p9|||Table 3 on p9.||||||18-DEC-06
19323|Wallumbilla Formation|30104|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|30443|6|Mentioned|p2|||See also P4. Aptian age||||||
19323|Wallumbilla Formation|30446|6|Mentioned|p39|||||||||
19323|Wallumbilla Formation|30458|6|Mentioned|p7|||Cretaceous age||||||
19323|Wallumbilla Formation|30508|6|Mentioned|p92|||Stratigraphic drilling||||||
19323|Wallumbilla Formation|30584|4|Described|Table 1|||||||||
19323|Wallumbilla Formation|30585|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|30587|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|30691|4|Described|Table 4|||Lower-Upper Cretaceous age. Of Rolling Downs Group||||||
19323|Wallumbilla Formation|30692|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|30694|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|Lower Cretaceous age||||||
19323|Wallumbilla Formation|30695|4|Described|Table 4|||Lower Cretaceous age.||||||17-SEP-08
19323|Wallumbilla Formation|30696|4|Described|Table 4|||Aptian-Albian age||||||
19323|Wallumbilla Formation|30698|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|30700|6|Mentioned|p22|||Lower Cretaceous age. Map||||||
19323|Wallumbilla Formation|30701|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|30702|6|Mentioned|Table 1|||Stratigraphic table||||||
19323|Wallumbilla Formation|30804|6|Mentioned|Table 2|||||||||
19323|Wallumbilla Formation|30853|5|Briefly described|Table 3|||Aptian to Lower Albian age||||||
19323|Wallumbilla Formation|30854|4|Described|Table 4|||Lower Cretaceous age||||||
19323|Wallumbilla Formation|30855|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|Unit in Rolling Downs Group||||||
19323|Wallumbilla Formation|30856|4|Described|Table 3|||Lower Cretaceous age.||||||
19323|Wallumbilla Formation|30857|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|30914|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
19323|Wallumbilla Formation|30915|6|Mentioned|Table|||Shown on stratigraphic table||||||
19323|Wallumbilla Formation|31097|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|31098|5|Briefly described|Table 1|||L. Cretaceous||||||
19323|Wallumbilla Formation|31116|4|Described|p43|||See also Table 2. Cretaceous||||||
19323|Wallumbilla Formation|31120|6|Mentioned|Table|||||||||
19323|Wallumbilla Formation|31121|6|Mentioned|Table 1|||||||||
19323|Wallumbilla Formation|31144|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|31145|5|Briefly described|Table 1|||L. Cretaceous||||||
19323|Wallumbilla Formation|31164|5|Briefly described|p8|||Aptian - Lower Albian, See also P10.||||||
19323|Wallumbilla Formation|31165|6|Mentioned|Table 11|||||||||
19323|Wallumbilla Formation|31168|6|Mentioned|p10|||||||||
19323|Wallumbilla Formation|31208|6|Mentioned|Fig 36|||See also Table 1||||||
19323|Wallumbilla Formation|31209|4|Described|p159|||||||||
19323|Wallumbilla Formation|31376|6|Mentioned|p4|||||||||
19323|Wallumbilla Formation|31422|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Of the Rolling Downs Group.  Mudstone, minor limestone, glauconitic sandstone.||||||02-DEC-04
19323|Wallumbilla Formation|31425|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|31430|5|Briefly described|Table 1|||L.Cretaceous||||||
19323|Wallumbilla Formation|31431|5|Briefly described|Table 3|||L.Cretaceous||||||
19323|Wallumbilla Formation|31432|4|Described|Table 1|||L.Cretaceous||||||
19323|Wallumbilla Formation|31433|5|Briefly described|p6|||L.Cretaceous||||||
19323|Wallumbilla Formation|31434|3|Fully described|Table 1|||See also p8. L.Cretaceous.||||||17-SEP-08
19323|Wallumbilla Formation|31436|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|31437|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|31438|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|31440|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|31441|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|31443|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|31553|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|31832|6|Mentioned|Table 6|||||||||
19323|Wallumbilla Formation|32136|6|Mentioned|p3|||Continuously cored composite section||||||
19323|Wallumbilla Formation|32193|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|32274|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|32275|4|Described|p8|||||||||
19323|Wallumbilla Formation|32276|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|32313|6|Mentioned|p165|||||||||
19323|Wallumbilla Formation|32314|6|Mentioned|Fig. 4|||||||||
19323|Wallumbilla Formation|32392|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|32393|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|32395|6|Mentioned|p6|||Stratigraphic table||||||
19323|Wallumbilla Formation|32396|6|Mentioned|p8|||Stratigraphic table||||||
19323|Wallumbilla Formation|32490|6|Mentioned|p9|||Crops out W of Buchanan sheet||||||
19323|Wallumbilla Formation|32553|4|Described|p38|||||||||
19323|Wallumbilla Formation|32705|6|Mentioned|p188|||||||||
19323|Wallumbilla Formation|32796|6|Mentioned|p302|||||||||
19323|Wallumbilla Formation|32797|4|Described|Table 4|||L.Cret.||||||
19323|Wallumbilla Formation|33016|6|Mentioned|p1|||On table||||||
19323|Wallumbilla Formation|33017|6|Mentioned|p5|||||||||
19323|Wallumbilla Formation|33067|4|Described|Table 1|Early Cretaceous|Early Cretaceous|Of the Rolling Downs Group.  Mudstone, siltstone,minor sandstone.||||||07-JUL-04
19323|Wallumbilla Formation|33069|4|Described|p7|||L.Cret.||||||
19323|Wallumbilla Formation|33070|4|Described|Table 2|||L.Cret.||||||
19323|Wallumbilla Formation|33071|4|Described|p2|||L.Cret.||||||
19323|Wallumbilla Formation|33072|4|Described|Table 1|||L.Cret.||||||
19323|Wallumbilla Formation|33073|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|33075|6|Mentioned|p445|||||||||
19323|Wallumbilla Formation|33078|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|33079|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|33080|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|33082|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|33083|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|33086|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower to Upper Cretaceous||||||
19323|Wallumbilla Formation|33087|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|33088|4|Described|Table 3|||||||||
19323|Wallumbilla Formation|33089|4|Described|Table 2|||L.Cret.||||||
19323|Wallumbilla Formation|33090|4|Described|Table 4|||L.Cret.||||||
19323|Wallumbilla Formation|33091|5|Briefly described|p9|||Stratigraphy||||||
19323|Wallumbilla Formation|33092|5|Briefly described|p6|||Strat. table||||||
19323|Wallumbilla Formation|33094|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|33095|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|33096|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|33150|4|Described|p9|||L.Cret.||||||
19323|Wallumbilla Formation|33151|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|33165|6|Mentioned|Chart|||Correlatin chart only||||||
19323|Wallumbilla Formation|33175|6|Mentioned|p280|||||||||
19323|Wallumbilla Formation|33176|5|Briefly described|p172|||||||||
19323|Wallumbilla Formation|33177|6|Mentioned|p12|||||||||
19323|Wallumbilla Formation|33178|6|Mentioned|p11|||||||||
19323|Wallumbilla Formation|33179|4|Described|Table 2|||||||||
19323|Wallumbilla Formation|33180|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|33182|6|Mentioned|p190|||||||||
19323|Wallumbilla Formation|33183|6|Mentioned|p233|||||||||
19323|Wallumbilla Formation|33368|6|Mentioned|p24|||Geol.Map.||||||
19323|Wallumbilla Formation|33372|4|Described|p17|||See also p20. From QDM Aramac 1.||||||18-DEC-06
19323|Wallumbilla Formation|33414|6|Mentioned|p212-214,Tb.||Aptian|Part of Wilgunya Sub-Group..||||||
19323|Wallumbilla Formation|33448|4|Described|Table 1|||L.Cret.||||||11-JAN-10
19323|Wallumbilla Formation|33449|4|Described|Table 1|||L.Cret.||||||
19323|Wallumbilla Formation|33451|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|33452|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|33561|6|Mentioned|p102|||||||||
19323|Wallumbilla Formation|33638|5|Briefly described|Table 1|||||||||
19323|Wallumbilla Formation|33639|5|Briefly described|p11|||L.Cret.||||||
19323|Wallumbilla Formation|33640|4|Described|Table 2|||||||||
19323|Wallumbilla Formation|33642|1|Redefined|p148|Early Cretaceous|Early Cretaceous|Includes Doncaster, Jones Valley, Ranmoor and Coreena Members. Contains Roma and older part of Tambo fauna of Aptian and Albian (Lower Cret)||||||
19323|Wallumbilla Formation|33643|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|33644|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|33645|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|33646|6|Mentioned|p8|||Strat. table.||||||
19323|Wallumbilla Formation|33647|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|33648|6|Mentioned|p20|||||||||
19323|Wallumbilla Formation|33672|5|Briefly described|p44|||Lithology.||||||
19323|Wallumbilla Formation|33673|4|Described|p292|||||||||
19323|Wallumbilla Formation|33772|6|Mentioned|p17|||||||||
19323|Wallumbilla Formation|33773|6|Mentioned|p17|||||||||
19323|Wallumbilla Formation|33825|6|Mentioned|p10|||Correlation table||||||
19323|Wallumbilla Formation|33832|5|Briefly described|p11|||Strat. and correlation.||||||18-DEC-06
19323|Wallumbilla Formation|33900|6|Mentioned|p21|||||||||
19323|Wallumbilla Formation|33939|6|Mentioned|p412|||||||||
19323|Wallumbilla Formation|33964|4|Described|p6|||Refers Vine et al. (1967).||||||
19323|Wallumbilla Formation|34065|4|Described|p6|||L.Cret.||||||
19323|Wallumbilla Formation|34091|5|Briefly described|Table 1|||See also P4. L.Cret. Part of Rolling Downs Group.||||||
19323|Wallumbilla Formation|34174|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|34212|6|Mentioned|p2|||Cretaceous||||||
19323|Wallumbilla Formation|34217|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|34218|4|Described|Table 1|||See also Table 2. Lower Cretaceous||||||
19323|Wallumbilla Formation|34356|6|Mentioned|p13|||Lower Cretaceous.||||||
19323|Wallumbilla Formation|34485|5|Briefly described|Table 1,p10|||Lower Cretaceous||||||
19323|Wallumbilla Formation|34486|5|Briefly described|Table 1|||Lower Cretaceous. See also Table 2||||||
19323|Wallumbilla Formation|34487|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|34611|6|Mentioned|Fig.65|||Correlation chart.||||||
19323|Wallumbilla Formation|34613|4|Described|Table 4|||||||||
19323|Wallumbilla Formation|34811|4|Described|Table 1|||||||||
19323|Wallumbilla Formation|35121|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|35139|4|Described|Table.2|||||||||
19323|Wallumbilla Formation|35239|6|Mentioned|p258|||||||||
19323|Wallumbilla Formation|35253|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|35457|6|Mentioned|Fig.5|||Stratigraphic correlation||||||
19323|Wallumbilla Formation|35560|4|Described|p290|||||||||
19323|Wallumbilla Formation|35640|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|35663|6|Mentioned|Fig.2|||Subsurface correlations of the central basin rock units.||||||
19323|Wallumbilla Formation|35793|6|Mentioned|Fig.3|||||||||
19323|Wallumbilla Formation|35811|5|Briefly described|Table 3|||||||||
19323|Wallumbilla Formation|35855|6|Mentioned|Fig.2|||Early Cretaceous lithostratigraphy.||||||
19323|Wallumbilla Formation|35936|6|Mentioned|p615|||||||||
19323|Wallumbilla Formation|35937|6|Mentioned|Fig.5|||||||||
19323|Wallumbilla Formation|36012|3|Fully described|Table 5|||See also p18.||||||18-DEC-06
19323|Wallumbilla Formation|36228|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|36243|6|Mentioned|Table 6A|||||||||
19323|Wallumbilla Formation|36251|4|Described|p3|||||||||
19323|Wallumbilla Formation|36570|5|Briefly described|p50|||See also p60.||||||18-DEC-06
19323|Wallumbilla Formation|36571|6|Mentioned|p101|||See also Table 4.||||||
19323|Wallumbilla Formation|36574|6|Mentioned|p602|||||||||
19323|Wallumbilla Formation|36580|6|Mentioned|Fig.2|||||||||
19323|Wallumbilla Formation|36581|6|Mentioned|p464|||||||||
19323|Wallumbilla Formation|36910|6|Mentioned|p61|||||||||
19323|Wallumbilla Formation|37117|5|Briefly described|p313|||||||||
19323|Wallumbilla Formation|37451|6|Mentioned|Table 2|||||||||
19323|Wallumbilla Formation|37597|6|Mentioned|p77|||||||||
19323|Wallumbilla Formation|37608|3|Fully described|Table 1 p316-319|||||||||
19323|Wallumbilla Formation|37995|4|Described|p66|||||||||
19323|Wallumbilla Formation|38199|5|Briefly described|p423|||Palynology||||||
19323|Wallumbilla Formation|38218|5|Briefly described|p289|||||||||
19323|Wallumbilla Formation|38226|6|Mentioned|Table 1|||||||||
19323|Wallumbilla Formation|38372|6|Mentioned|p651|||||||||
19323|Wallumbilla Formation|38373|6|Mentioned|p619|||||||||
19323|Wallumbilla Formation|38608|6|Mentioned|Map legend|Mesozoic|Mesozoic|||||||
19323|Wallumbilla Formation|38779|6|Mentioned|p7|||||||||
19323|Wallumbilla Formation|38780|6|Mentioned|p17|||||||||
19323|Wallumbilla Formation|38814|6|Mentioned|Table 1|||||||||
19323|Wallumbilla Formation|39029|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Overlies Gilbert River Formation.||||||25-AUG-04
19323|Wallumbilla Formation|39070|4|Described|p364|||||||||
19323|Wallumbilla Formation|39211|5|Briefly described|Fig.3|||See also Figs 4,7,9,11-15 etc. Correlation||||||
19323|Wallumbilla Formation|39212|6|Mentioned|p18|||||||||
19323|Wallumbilla Formation|39216|6|Mentioned|p55|||||||||
19323|Wallumbilla Formation|39445|5|Briefly described|Table 11|||||||||
19323|Wallumbilla Formation|39478|6|Mentioned|Table 1|||||||||
19323|Wallumbilla Formation|39556|5|Briefly described|Map legend|Cretaceous|Cretaceous|||||||
19323|Wallumbilla Formation|39627|6|Mentioned|p269|||||||||
19323|Wallumbilla Formation|39708|6|Mentioned|p478|||||||||
19323|Wallumbilla Formation|39797|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|39799|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|39846|6|Mentioned|p44|||||||||
19323|Wallumbilla Formation|39847|5|Briefly described|p38|||||||||
19323|Wallumbilla Formation|39899|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
19323|Wallumbilla Formation|39917|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|39942|6|Mentioned|p468|||||||||
19323|Wallumbilla Formation|39943|6|Mentioned|Table 8A|||||||||
19323|Wallumbilla Formation|39988|6|Mentioned|p288|||||||||
19323|Wallumbilla Formation|39989|4|Described|p423|||||||||
19323|Wallumbilla Formation|40058|6|Mentioned|p2|||||||||
19323|Wallumbilla Formation|40121|6|Mentioned|Table 1|||||||||
19323|Wallumbilla Formation|40150|6|Mentioned|p81|||||||||
19323|Wallumbilla Formation|40199|6|Mentioned|Fig.1|||||||||
19323|Wallumbilla Formation|40218|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
19323|Wallumbilla Formation|40245|6|Mentioned|Table 2|||||||||
19323|Wallumbilla Formation|40249|6|Mentioned|p38|||Mention P41||||||
19323|Wallumbilla Formation|40250|6|Mentioned|Fig.1|||||||||
19323|Wallumbilla Formation|40452|6|Mentioned|p2|||||||||
19323|Wallumbilla Formation|40541|3|Fully described|p111|||||||||
19323|Wallumbilla Formation|40544|6|Mentioned|p159|||||||||
19323|Wallumbilla Formation|40623|5|Briefly described|p108|||||||||
19323|Wallumbilla Formation|40648|6|Mentioned|p12|||||||||
19323|Wallumbilla Formation|40659|6|Mentioned|p250|||||||||
19323|Wallumbilla Formation|40666|4|Described|p358|||||||||
19323|Wallumbilla Formation|40670|6|Mentioned|Fig.9|||||||||
19323|Wallumbilla Formation|40675|6|Mentioned|Table 8A|||||||||
19323|Wallumbilla Formation|40687|3|Fully described|p418|||||||||
19323|Wallumbilla Formation|40771|6|Mentioned|p429|||||||||
19323|Wallumbilla Formation|40801|6|Mentioned|p29|||See also P39||||||
19323|Wallumbilla Formation|40832|3|Fully described|p457|||||||||
19323|Wallumbilla Formation|40833|6|Mentioned|p468|||||||||
19323|Wallumbilla Formation|40926|6|Mentioned|p18|||||||||
19323|Wallumbilla Formation|40962|6|Mentioned|Table 1|||||||||
19323|Wallumbilla Formation|41012|5|Briefly described|p137|||||||||
19323|Wallumbilla Formation|41060|6|Mentioned|Fig.3|||Generalized stratigraphy||||||
19323|Wallumbilla Formation|41062|6|Mentioned|Fig.5|||||||||
19323|Wallumbilla Formation|41063|6|Mentioned|p40|||||||||
19323|Wallumbilla Formation|41064|6|Mentioned|p60|||||||||
19323|Wallumbilla Formation|41084|5|Briefly described|Fig.2|||||||||
19323|Wallumbilla Formation|41086|3|Fully described|p98, Fig.3|||Mentioned p101.||||||18-DEC-06
19323|Wallumbilla Formation|41087|6|Mentioned|p123|||||||||
19323|Wallumbilla Formation|41088|6|Mentioned|p141|||||||||
19323|Wallumbilla Formation|41097|6|Mentioned|p165|||||||||
19323|Wallumbilla Formation|41099|6|Mentioned|Fig.9|||||||||
19323|Wallumbilla Formation|41117|6|Mentioned|Fig.2|||||||||
19323|Wallumbilla Formation|41165|5|Briefly described|p362|||||||||
19323|Wallumbilla Formation|41175|6|Mentioned|Fig.1|||||||||
19323|Wallumbilla Formation|41176|6|Mentioned|Table 2|||||||||
19323|Wallumbilla Formation|41177|6|Mentioned|p225|||||||||
19323|Wallumbilla Formation|41178|6|Mentioned|p242|||||||||
19323|Wallumbilla Formation|41182|5|Briefly described|p289|||||||||
19323|Wallumbilla Formation|41183|6|Mentioned|p310|||||||||
19323|Wallumbilla Formation|41184|6|Mentioned|p347|||||||||
19323|Wallumbilla Formation|41186|6|Mentioned|p197|||||||||
19323|Wallumbilla Formation|41187|6|Mentioned|p227|||||||||
19323|Wallumbilla Formation|41196|6|Mentioned|Fig.1|||||||||
19323|Wallumbilla Formation|41198|6|Mentioned|Table 1|||||||||
19323|Wallumbilla Formation|41214|6|Mentioned|Fig.3|||||||||
19323|Wallumbilla Formation|41216|6|Mentioned|Fig.18|||||||||
19323|Wallumbilla Formation|41246|6|Mentioned|Map legend|Cretaceous||||||||
19323|Wallumbilla Formation|41266|6|Mentioned|Fig.3|||||||||
19323|Wallumbilla Formation|41286|6|Mentioned|p118|||||||||
19323|Wallumbilla Formation|41306|6|Mentioned|p4|||||||||
19323|Wallumbilla Formation|41307|6|Mentioned|p5|||||||||
19323|Wallumbilla Formation|41361|6|Mentioned|Fig.3|||||||||
19323|Wallumbilla Formation|41427|6|Mentioned|p84|||||||||
19323|Wallumbilla Formation|41464|6|Mentioned|Map legend|Early Cretaceous||||||||
19323|Wallumbilla Formation|41523|3|Fully described|p278|||||||||
19323|Wallumbilla Formation|41556|6|Mentioned|Map legend|Early Cretaceous||||||||
19323|Wallumbilla Formation|41568|5|Briefly described|p15|||||||||
19323|Wallumbilla Formation|41681|6|Mentioned|p11,p22|||||||||
19323|Wallumbilla Formation|41707|6|Mentioned|p164|||||||||
19323|Wallumbilla Formation|41992|4|Described|Fig.2 p183|||||||||26-APR-18
19323|Wallumbilla Formation|42007|5|Briefly described|p182|||||||||
19323|Wallumbilla Formation|42061|4|Described|p157|||See also Fig.11||||||
19323|Wallumbilla Formation|42067|5|Briefly described|p309|||See also Appendix 2||||||
19323|Wallumbilla Formation|42071|6|Mentioned|p117|||||||||
19323|Wallumbilla Formation|42084|6|Mentioned|Fig.3 P356|||||||||
19323|Wallumbilla Formation|42085|6|Mentioned|Fig.2 P374|||||||||
19323|Wallumbilla Formation|42369|5|Briefly described|Fig.10, P61|||||||||
19323|Wallumbilla Formation|42397|6|Mentioned|Fig.2 P3|||||||||
19323|Wallumbilla Formation|42429|5|Briefly described|Fig.3 P155|||||||||
19323|Wallumbilla Formation|42446|4|Described|p13|||||||||
19323|Wallumbilla Formation|42447|6|Mentioned|p16|||||||||
19323|Wallumbilla Formation|42474|5|Briefly described|p25|||||||||
19323|Wallumbilla Formation|42496|5|Briefly described|p136, Fig.3 p132|||||||||
19323|Wallumbilla Formation|42520|5|Briefly described|p6|||||||||
19323|Wallumbilla Formation|42634|6|Mentioned|Table 8 P34|||||||||
19323|Wallumbilla Formation|42637|4|Described|p10, 23|||||||||
19323|Wallumbilla Formation|42673|5|Briefly described|Fig.2, P184|||||||||
19323|Wallumbilla Formation|42746|6|Mentioned|Fig.6 P8|||||||||
19323|Wallumbilla Formation|42749|5|Briefly described|p31|||see also Fig.2 p27.||||||18-DEC-06
19323|Wallumbilla Formation|42804|5|Briefly described|p115|||||||||
19323|Wallumbilla Formation|42940|5|Briefly described|Plate 2|Mesozoic|Mesozoic|Siltstone, porcellanite, sandstone; marine fossils.  Geological province: Amadeus Basin.||||||23-JAN-08
19323|Wallumbilla Formation|42999|5|Briefly described|Table 2,p90||Early Cretaceous|||||||
19323|Wallumbilla Formation|43000|5|Briefly described|p114|||see also Fig.5,p112||||||
19323|Wallumbilla Formation|43002|5|Briefly described|Fig.2,p135|||||||||
19323|Wallumbilla Formation|43004|5|Briefly described|Table 1,p179|||||||||
19323|Wallumbilla Formation|43083|5|Briefly described|p185|Cretaceous|Cretaceous|Argillaceouis deposits.||||||17-JUN-09
19323|Wallumbilla Formation|43105|5|Briefly described|Fig.9,p15.|||||||||
19323|Wallumbilla Formation|43114|5|Briefly described|p14|||||||||
19323|Wallumbilla Formation|43122|5|Briefly described|p25|||see also Fig. 2.||||||
19323|Wallumbilla Formation|43254|5|Briefly described|map legend|Early Cretaceous|Late Jurassic|||||||
19323|Wallumbilla Formation|43285|5|Briefly described|Map Legend|Early Cretaceous|Late Jurassic|||||||
19323|Wallumbilla Formation|43287|5|Briefly described|Map Legend||Early Cretaceous|||||||
19323|Wallumbilla Formation|43404|14|Not recorded|Table p11||Cretaceous|||||||
19323|Wallumbilla Formation|43564|6|Mentioned|p453||Aptian|(Late Aptian)||||||
19323|Wallumbilla Formation|43591|6|Mentioned|p40|||||||||
19323|Wallumbilla Formation|43602|4|Described|191|||In the Eromanga Basin. Of the Rolling Downs Group.||||||18-DEC-06
19323|Wallumbilla Formation|43625|6|Mentioned|p48,74|||||||||
19323|Wallumbilla Formation|43630|6|Mentioned|p69, fig.4|||||||||
19323|Wallumbilla Formation|43989|14|Not recorded|Map Legend||Early Cretaceous|||||||
19323|Wallumbilla Formation|44016|14|Not recorded|Map Legend||Early Cretaceous|||||||
19323|Wallumbilla Formation|44017|14|Not recorded|Map Legend||Early Cretaceous|||||||
19323|Wallumbilla Formation|44018|14|Not recorded|Map Legend||Early Cretaceous|||||||
19323|Wallumbilla Formation|44019|14|Not recorded|Map Legend||Early Cretaceous|||||||
19323|Wallumbilla Formation|44020|14|Not recorded|Tb.1,2||Early Cretaceous|Of Rolling Downs Group.||||||
19323|Wallumbilla Formation|44031|14|Not recorded|p3,8,9,11,12||Cretaceous|||||||
19323|Wallumbilla Formation|44034|4|Described|Tb.2,p2,5,7-10,Fig.1|||||||||
19323|Wallumbilla Formation|44042|14|Not recorded|Map Legend||Early Cretaceous|||||||
19323|Wallumbilla Formation|44082|6|Mentioned|p3,4,6,8,10-30,Tb.34||Early Cretaceous|Mentioned with respect to Qld Cretaceous fossils which are either of stratigraphic significance or are illustrative of the occurrence of a particular group.||||||
19323|Wallumbilla Formation|44091|14|Not recorded|p60,63||Cretaceous|||||||
19323|Wallumbilla Formation|44099|14|Not recorded|Map Legend||Early Cretaceous|(Rolling Downs Group)||||||
19323|Wallumbilla Formation|44112|6|Mentioned|p82|||||||||
19323|Wallumbilla Formation|44133|5|Briefly described|p104 Fig. 9.11|Cretaceous|Cretaceous|Geological Province: Eromanga Basin.||||||
19323|Wallumbilla Formation|44308|14|Not recorded|p11,|||||||||
19323|Wallumbilla Formation|44376|14|Not recorded|p3|||||||||
19323|Wallumbilla Formation|44410|14|Not recorded|Map Legend||Early Cretaceous|||||||
19323|Wallumbilla Formation|44637|14|Not recorded|p287-291||Cretaceous|||||||
19323|Wallumbilla Formation|44807|14|Not recorded|p9|||Correlated with Blackdown Formation.||||||
19323|Wallumbilla Formation|45022|6|Mentioned|p111|Albian|Aptian|||||||
19323|Wallumbilla Formation|45071|6|Mentioned|p79|||||||||
19323|Wallumbilla Formation|45110|6|Mentioned|p24|||See also Table 18.||||||
19323|Wallumbilla Formation|45132|6|Mentioned|Table 2|||See also Fig.1.||||||
19323|Wallumbilla Formation|45145|3|Fully described|Table 5|||||||||
19323|Wallumbilla Formation|45161|6|Mentioned|p67|||||||||
19323|Wallumbilla Formation|46791|4|Described|p44|||||||||
19323|Wallumbilla Formation|46881|6|Mentioned|p198|||||||||
19323|Wallumbilla Formation|46902|6|Mentioned|p36|||||||||
19323|Wallumbilla Formation|46937|6|Mentioned|Fig.10|||||||||
19323|Wallumbilla Formation|46939|6|Mentioned|Fig.2|||See also Fig.1.||||||
19323|Wallumbilla Formation|46984|6|Mentioned|Table 1|||||||||
19323|Wallumbilla Formation|47042|6|Mentioned|p171|||||||||
19323|Wallumbilla Formation|47083|5|Briefly described|p20||Mesozoic|Of Rolling Downs Group.||||||
19323|Wallumbilla Formation|48919|6|Mentioned|p71|||Cretaceous. See also P72||||||
19323|Wallumbilla Formation|48920|3|Fully described|p58|||Lower Cretaceous age||||||
19323|Wallumbilla Formation|48951|6|Mentioned|Table 1|||||||||
19323|Wallumbilla Formation|49010|6|Mentioned|Fig.4|||Eromanga Basin||||||
19323|Wallumbilla Formation|49011|6|Mentioned|Fig.3|||Eromanga Basin||||||
19323|Wallumbilla Formation|50100|5|Briefly described|p23|Cretaceous|Cretaceous|Of the Rolling Downs Group.  Geological Province: Eromanga Basin.||||||
19323|Wallumbilla Formation|50199|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|50332|5|Briefly described|p22, p78|Mesozoic|Mesozoic|Geological Province: Carpentaria Basin. Main lithologies are mudstone, calcareous shale, limestone, sandstone and siltstone.||||||07-FEB-11
19323|Wallumbilla Formation|50627|5|Briefly described|Map legend|Cretaceous|Cretaceous|Clay-rich mudstone, silty mudstone, sandy siltstone, and sandstone.||||||
19323|Wallumbilla Formation|60081|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Mudstone and quartz-poor sandstone, minor glauconitic sandstone.||||||
19323|Wallumbilla Formation|60087|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Of the Rolling Downs Group. Mudstone, minor labile and galuconitic sandstone, limestone.||||||
19323|Wallumbilla Formation|60281|5|Briefly described|p27|Early Cretaceous|Early Cretaceous|Geological Province: Clarence-Moreton Basin, Cecil Plains Sub-basin.||||||20-JAN-05
19323|Wallumbilla Formation|60331|5|Briefly described|p34 Fig.3|Albian|Aptian|Overlies Gilbert River Formation. Overlain by Toolebuc Formation. Geological Province: Eromanga Basin.||||||
19323|Wallumbilla Formation|60357|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|Overlies: Coffin Hill Member (Gilbert River Formation). Mudstone and siltstone, minor sandstone. Geological Province: Carpentaria Basin.||||||20-AUG-04
19323|Wallumbilla Formation|60358|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|Silty and sandy claystone, mudstone and siltstone, calcareous concretions; minor glauconitic sandstone. Geological Province: Laura Basin.||||||18-AUG-04
19323|Wallumbilla Formation|60359|5|Briefly described|Map Legend|Mesozoic|Mesozoic|Mudstone, siltstone.||||||
19323|Wallumbilla Formation|60524|5|Briefly described|p486 Fig. 1, p488|Albian|Aptian|Marine deposits; contains Viviparidae fossils.  Geological Province: Eromanga Basin.||||||
19323|Wallumbilla Formation|60717|5|Briefly described|p40 Fig. 2|Early Cretaceous|Early Cretaceous|Overlies Cadna-owie Formation. Overlain by Toolebuc Formation. Lateral to Bulldog Shale. Geological Province: Eromanga Basin.||||||31-JAN-08
19323|Wallumbilla Formation|61014|6|Mentioned|p533 Fig.2, p539. |Early Cretaceous|Early Cretaceous|Eromanga Basin.||||Overlies Wyandra Sandstone Member. Is overlain by Allaru Mudstone.||
19323|Wallumbilla Formation|61312|4|Described|p64, p67 Fig. E5, p73-74|Early Cretaceous|Early Cretaceous|Of Rolling Downs Gp. Marine sediment sequence of mudstone and siltstone, with limestone, minor lenticular sandstone, and intraformational conglomerate. Overlies Cadna-owie Fm.; overlain by Toolebuc Fm in Qld. Thickness: 300m. Geol. Prov: Eromanga Basin.||||||
19323|Wallumbilla Formation|61377|5|Briefly described|p148 Tb. SU1|Early Cretaceous|Early Cretaceous|Of the Rolling Downs Group. Mudstone, siltstone, minor sandstone, coal, conglomerate. Overlies Pilliga Sandstone. Geological Province: Surat Basin.||||||07-FEB-11
19323|Wallumbilla Formation|61611|6|Mentioned|p265 Fig. 3|Early Cretaceous|Early Cretaceous|Geological Province: Surat Basin and Eromanga Basin.||||||13-MAR-09
19323|Wallumbilla Formation|61613|6|Mentioned|p282 Fig. 2|Early Cretaceous|Early Cretaceous|Of Maree Subgroup. Geological Province: Eromanga Basin.||||||07-FEB-11
19323|Wallumbilla Formation|61614|6|Mentioned|p290 Fig. 2|Early Cretaceous|Early Cretaceous|Geological Province: Eromanga Basin.||||||17-MAR-09
19323|Wallumbilla Formation|62028|5|Briefly described|p10 Fig. 1|||||||||
19323|Wallumbilla Formation|62029|5|Briefly described|p15|Cretaceous|Cretaceous|Siltstone and shale - impermeable and acts as reservoir seal. See also Fig. 4.||||||14-APR-08
19323|Wallumbilla Formation|62376|5|Briefly described|p84|Early Cretaceous|Early Cretaceous|Geological Province: Pedirka Basin.||||||09-FEB-10
19323|Wallumbilla Formation|62537|6|Mentioned|p191 Fig.2. |Early Cretaceous|Early Cretaceous|Eromanga Basin.||||Overlies Cadna-owie Formation. Is overlain by Coorikiana Formation.||
19323|Wallumbilla Formation|62730|5|Briefly described|p352 Fig. 1|Cretaceous|Cretaceous|Geological Province: Eromanga Basin.||||||21-APR-08
19323|Wallumbilla Formation|62837|5|Briefly described|Stratigraphic columns|Early Cretaceous|Early Cretaceous|Of the Rolling Downs Group. Age: ~113-~98Ma. Geological Province: Northern Gulf of Carpentaria.||||||01-MAR-10
19323|Wallumbilla Formation|63218|6|Mentioned|p211 Fig.2. |Early Cretaceous|Early Cretaceous|Surat Basin.|||Includes Doncaster and Coreena Members.|Overlies Bungil Formation. Is overlain by Surat Siltstone.||
19323|Wallumbilla Formation|63979|1|Redefined|p48, Fig. 44|Albian|Barremian|Lower part of Wilgunya Subgp.Equates to Bulldog Shale, Coorikiana Sst.+lower part of Oodnadatta Fm in SA. Informally subdiv.into lower+upper Wallumbilla Fm.Contains Doncaster +Coreena Members.Conformable on Cadna-owie Fm. Thickness:350m.Detailed lith.||||||03-DEC-18
19323|Wallumbilla Formation|64048|5|Briefly described|p64 Tb. 2|Early Cretaceous|Early Cretaceous|Contains the Coreena Member. Geological Province: Eromanga Basin.||||||07-FEB-11
19323|Wallumbilla Formation|64197|6|Mentioned|p625 Fig.1c, p630 Figs.6,7|Cretaceous|Cretaceous|Eromanga and Surat Basins.||Unit in Marree Subgroup.||Eromanga Basin: underlies Toolebuc Formation; overlies Cadna-owie Formation. Surat Basin: underlies the Surat Siltstone, overlies the Bungil Formation.||11-DEC-15
19323|Wallumbilla Formation|64665|6|Mentioned|p62.|Cretaceous|Cretaceous|Eromanga Basin.||||||
19323|Wallumbilla Formation|64820|5|Briefly described|pS6 Fig. 4|Barremian|Albian|Of the Rolling Downs Group. Geological province: Weipa Sub-basin, Carpentaria Basin.||||||
19323|Wallumbilla Formation|64856|3|Fully described|p79, p98-101|Albian|Aptian|Named and defined in the Surat Basin by Vine et al. (1967), with the type section in Wallumbilla Creek, near Roma. Also in Eromanga Basin. Contains Doncaster and Coreena Members. Conformably overlies Bungil Formation. Age from pollen assemblages (units APK3, 4). Mudstone, siltstone, concretionary limestone, minor lenticular sandstone, conglomerate. Up to 475m thick.|| ||||29-NOV-17
19323|Wallumbilla Formation|64857|5|Briefly described|p113 Fig.3|||Overlies Bungil Formation, Surat Basin.||||||
19323|Wallumbilla Formation|64858|6|Mentioned|p181 Tb.1, p187-188|||Surat Basin.||||||30-NOV-09
19323|Wallumbilla Formation|65112|6|Mentioned|Fig 11 p324; Fig 16 p 328|Early Cretaceous|Early Cretaceous|Unit in the Surat Basin.|||Includes Doncaster and Coreena Members.|Overlies the Bungil Formation; underlies the Surat Siltstone.||22-MAR-12
19323|Wallumbilla Formation|65113|5|Briefly described|Fig 4 p340|Early Cretaceous|Early Cretaceous|Overlies the Bungil Formation, Surat Siltstone.||||||
19323|Wallumbilla Formation|65114|5|Briefly described|p385 Fig.3|Early Cretaceous||||||||
19323|Wallumbilla Formation|65116|5|Briefly described|Fig 2 p437|Early Cretaceous|Early Cretaceous|Includes Coreena Member, Doncaster Member. Underlies the Surat Siltstone, Overlies the Bungil Formation, Surat Basin.||||||
19323|Wallumbilla Formation|65119|5|Briefly described|p503, 504, fig 7-8 p514, Fig 16-19|Early Cretaceous|Early Cretaceous|Surat Basin. Marine shelf deposits of siltstone, mudstone and fine sandstone. Age: 111-117 Ma. Fission Track age: 87-109 Ma.||||||07-MAR-12
19323|Wallumbilla Formation|65238|5|Briefly described|p7 Fig. 8, p14 Fig. 17|Early Cretaceous|Early Cretaceous|Geological province: Eromanga Basin. Transgressive marine deposits.||||||
19323|Wallumbilla Formation|65384|6|Mentioned|S116, S118|||In Surat Basin? Includes Doncaster Member.||||||
19323|Wallumbilla Formation|65385|5|Briefly described|pS134 Fig.7|Early Cretaceous|Early Cretaceous|Of Eromanga Basin. Overlies Cadna-owie Formation. Overlain by Toolebuc Formation.||||||08-MAR-12
19323|Wallumbilla Formation|65489|5|Briefly described|p49, p55-56, p58, p61, p155|Early Cretaceous|Early Cretaceous|Eromanga Basin. 450m thick. Regional seal.||||Overlies Cadna-owie Formation. Is overlain by Toolebuc Formation.||
19323|Wallumbilla Formation|66529|6|Mentioned|p12 Fig.5|||||Unit in Rolling Downs Group.|Includes Doncaster, Coreena, Jones V and Ranmoor Members.|||
19323|Wallumbilla Formation|66623|3|Fully described|p239, pp242-245, pp256-259. |Albian|Aptian|Previously known as the Blackdown Formation in Queensland. c.360 m thick. Contains a wide range of fossils. Shoreline to deeper marine environment. Outcrops as low rolling hills. Hosts opals at White Cliffs; possible heavy mineral (magnetite and zircon) strandlines locally.||Unit in Rolling Downs Group.|Includes Coreena and Doncaster Members.|Conformably, but sharply overlies Wyandra Sandstone Member. Coreena Member is gradationally overlain by Allaru Mudstone. Doncaster Member disconformably overlies Cadna-owie Formation.|Muddy sandstone and siltstone with local large spherical calcareous concretions; black shale and minor sandstone with abundant dropstone boulders; pyritic and bioturbated mudstone, claystone and shale; calcareous and glauconitic sandstones.|05-JUN-13
19323|Wallumbilla Formation|66915|4|Described|p1-2, 4-6, p9, p11 Fig.7, p12, p16, p18|Cretaceous|Cretaceous|Carpentaria, Eromanga and Surat Basins. Base of Wallumbilla Formation (the "C-Horizon") and correlatives is the major bounding surface of the Great Artesian Basin.||Basal Rolling Downs Group|Coreena Member, Doncaster Member|Overlies Wyandra Sandstone Member (Cadna-owie Formation), Gilbert River and Bungil Formations.|Marine muds.|12-JAN-17
19323|Wallumbilla Formation|66920|5|Briefly described|Map legend|Cretaceous|Cretaceous|||Unit in Rolling Downs Group.|Includes Doncaster Member.||Marine grey mudstone and siltstone with minor interbeds of fine-grained glauconitic and calcareous sandstone, local thin micritic limestone beds and heavy mineral strandline accumulations; down-sequence glacial ice-rafted erratics.|
19323|Wallumbilla Formation|67133|5|Briefly described|p2, p5, p17-19|Early Cretaceous|Early Cretaceous|Samples of this unit were analysed by XRD and optical microscopy for this study. Consists of quartz (27-52%), feldspars (20-30%) with plagioclase dominant, minor (<8%) kaolinite and significant (13-26%) mixed-layer clays, mainly illite.|||Doncaster and Coreena Members.||Siltstones and mudstones with minor sandstones.|
19323|Wallumbilla Formation|67207|5|Briefly described|Map legend.|Cretaceous|Cretaceous|||Unit in Rolling Downs Group.|Includes Doncaster and Coreena Members.||Marine grey mudstone and siltstone with minor interbeds of fine-grained glauconitic and calcareous sandstone, local thin micritic limestone beds and heavy mineral strandline accumulations; down-sequence glacial ice-rafted erratics.|
19323|Wallumbilla Formation|67209|5|Briefly described|Map legend.|Cretaceous|Cretaceous|||Unit in Rolling Downs Group.|Includes Doncaster and Coreena Members.|Overlies Cadna-owie Formation. Is overlain by Allaru Mudstone.|Marine grey mudstone and siltstone with minor interbeds of fine-grained glauconitic and calcareous sandstone, local thin micritic limestone beds and heavy mineral strandline accumulations; down-sequence glacial ice-rafted erratics.|
19323|Wallumbilla Formation|67211|5|Briefly described|Map legend.|Cretaceous|Cretaceous|||Unit in Rolling Downs Group.|Includes Doncaster and Coreena Members.|Overlies Easter Monday Formation.|Marine grey mudstone and siltstone with minor interbeds of fine-grained glauconitic and calcareous sandstone, local thin micritic limestone beds and heavy mineral strandline accumulations; down-sequence glacial ice-rafted erratics.|
19323|Wallumbilla Formation|67323|5|Briefly described|p86-87, p92 Fig.12.2, p93, p94 Fig.12.4|Early Cretaceous|Early Cretaceous|See also GIS attrib tbl, Solid Geology Map, p95 Fig.12.5, p96. Eromanga/Carpentaria Basins. Marine sediments.|||Includes Ranmoor Member.|Overlies Cadna-owie and Gilbert River Formations and Longsight Sandstone. Is overlain by Toolebuc Formation.|Mudstone and siltstone with calcareous concretions.|
19323|Wallumbilla Formation|67402|4|Described|p26, p26 tbl RRM4, p29|Albian|Aptian|Eromanga Basin. Deposited in a transgressive marine environment which was followed by paralic and fluvial deposition. Ranges from 200 to over 350m thick in the Eromanga Basin and up to 600m thick in the Carpentaria Basin. Proven regional seal for hydrocarbons. Misspelt as Wullumbilla on p265. See also p29 fig PSA4, PSA5, p108-p112, p113 fig ERO12, p115 tbl ERO2, p120, P123, p146 fig SRT3, p148, p156, p176, p177, p179 fig CRP/KRM6, p181, p265.||Rolling Downs Group||Overlies the Cadna-owie Formation and Gilbert River Formation. Overlain by the Allaru Mudstone and Toolebuc Formation.|Consists primarily of marine mudstone interbedded with sandy mudstone, siltstone, shale and limestone.|
19323|Wallumbilla Formation|67561|5|Briefly described|p51-60, p62 Fig.11, p67, p68|Aptian|Aptian|Eromanga Basin. Australian Spore-Pollen zonation: C.hughesi. Deposited on a shallow marine shelf during a cold climate transgression. Previously regarded as a lowstand section, but re-interpreted by Bron (2010) as a tsunami deposit generated by the (125 +/- 1 Ma) Tookoonooka impact.||||Correlative of the Bulldog Shale.|Contains glendonites, petrified wood, and ice-rafted boulders of exotic lithology.|20-JAN-17
19323|Wallumbilla Formation|67669|5|Briefly described|p11|Early Cretaceous|Early Cretaceous|Of Bowen Basin.||Unit of Rolling Downs Group.||Underlain by Bungil Formation.||
19323|Wallumbilla Formation|67784|6|Mentioned|p25, p26, p28-29, p31, p32|||185-253m thick. Northern Eromanga Basin.||Wilgunya Subgroup.|Includes Doncaster Member, Jones Valley Member, Ranmoor Member, Coreena Member|Overlies Gilbert River Formation, overlain by Toolebuc Formation||08-FEB-18
19323|Wallumbilla Formation|68003|5|Briefly described|p57 Fig.3-n.|||Bowen Basin.||Unit in Rolling Downs Group.||Overlies Bungil Formation. Is overlain by Surat Siltstone.||
19323|Wallumbilla Formation|68004|6|Mentioned|p175.|||A seal for reservoirs in the Hooray and Mooga Sandstones.||||||
19323|Wallumbilla Formation|68069|5|Briefly described|Map legend.|Early Cretaceous|Early Cretaceous|Surat Basin. Shown on cross-sections and time-space plot and basement interpretation only.||Rolling Downs Group|Includes Coreena and Doncaster Members.|Overlies Bungil Formation. Is overlain conformably by Surat Siltstone.|Sandstone, claystone, siltstone and mudstone.|22-NOV-13
19323|Wallumbilla Formation|68117|5|Briefly described|p346|Early Cretaceous|Early Cretaceous|Surat Basin.|||Doncaster, Coreena Members.|||
19323|Wallumbilla Formation|68206|5|Briefly described|p31-33|Aptian|Aptian|Carpentaria, Eromanga Basins.|||Doncaster, Jones Valley, Ranmoor Members.|Is overlain by Toolebuc Formation.||
19323|Wallumbilla Formation|68279|6|Mentioned|p18-19|||Galilee Basin stratigraphic cross-sections, and mineralogy tables.||||||
19323|Wallumbilla Formation|68345|5|Briefly described|Map legend.|Early Cretaceous|Early Cretaceous|Carpentaria Basin.||||Conformably overlies Coffin Hill Member (Gilbert River Formation).|Mudstone and siltstone with calcareous concretions.|
19323|Wallumbilla Formation|68349|5|Briefly described|Map legend.|Early Cretaceous|Early Cretaceous|Carpentaria Basin.||||Conformably overlies Coffin Hill Member (Gilbert River Formation).|Mudstone and siltstone with calcareous concretions.|
19323|Wallumbilla Formation|68417|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|Carpentaria Basin. No outcrop in map area: shown only in subsurface and rock relationship diagram.||||Conformably underlain by the Coffin Hill Member, Gilbert River Formation.|Mudstone and siltstone with calcareous concretions.|
19323|Wallumbilla Formation|68553|6|Mentioned|Map legend; schematic diagram.|Cretaceous|Cretaceous|Surat, Eromanga, Laura and Carpentaria Basins.||Unit in Rolling Downs Group.||Is overlain conformably by Griman Creek Formation and Toolebuc Formation.||
19323|Wallumbilla Formation|68576|5|Briefly described|Q_4: p3|Early Cretaceous|Early Cretaceous|Surat Basin.|||Doncaster, Coreena Members.|Overlies Bungil Formation. Is overlain by Surat Siltstone.||
19323|Wallumbilla Formation|68593|5|Briefly described|p4, p47|Early Cretaceous|Early Cretaceous|Mainly marine deposits.|||Doncaster and Coreena Members.|Overlies Bungil Formation. Is overlain by Surat Siltstone.|Siltstone, mudstone, minor conglomerate, rare coal.|
19323|Wallumbilla Formation|68731|6|Mentioned|pp209-211|||||||||
19323|Wallumbilla Formation|68734|5|Briefly described|p218 Fig.2, p221 Fig.3|Aptian|Barremian|Eromanga Basin (NE). Marine to coastal paralic and shallow marine.||Of the Rolling Downs Group.|Includes Coreena Member and Doncaster Member.|||16-JAN-17
19323|Wallumbilla Formation|68821|5|Briefly described|p292 Fig.1, p292, p295, p296, p298|Cretaceous|Cretaceous|Lower Cretaceous age. Equivalent to the Bulldog Shale Formation. Parallic to marine sediments. Contains ubiquitous disseminated pyrite.||Of the Rolling Downs Group.|||Consist of pyrite and carbonaceous-rich marine mudstones and siltstones interbedded with fine sandstones.|
19323|Wallumbilla Formation|68901|5|Briefly described|p7 Fig. ii|Upper Cretaceous|Lower Cretaceous|Eromanga Basin.||Rolling Downs Group|||Mudstone, siltstone, sandstone; calcareous in part.|27-SEP-18
19323|Wallumbilla Formation|69019|5|Briefly described|p85 Fig.21.|Albian|Aptian|Southern Eromanga Basin.||||Overlies Cadna-owie Formation. Is overlain by Toolebuc Formation.||
19323|Wallumbilla Formation|69023|6|Mentioned|p89 Fig.20, p99|Albian|Aptian|||||||
19323|Wallumbilla Formation|69297|5|Briefly described|p273, p274 fig 4. 3, p275|Upper Cretaceous|Upper Jurassic|Carpentaria Basin. Contains good TOC for hydrocarbon generation.||Rolling Downs Group||Overlies the Gilbert River Formation. Overlain by the Toolebuc Formation.|Lithic glauconitic sandstones, siltstone, claystone and limestone.|
19323|Wallumbilla Formation|69377|5|Briefly described|map legend|Early Cretaceous|Early Cretaceous||||||Mudstone and siltstone with calcareous concretions|
19323|Wallumbilla Formation|69379|5|Briefly described|map legend|Cretaceous|Cretaceous||||Doncaster Member|||
19323|Wallumbilla Formation|69454|6|Mentioned|p38:3, 13|||Eromanga Basin. Potential seal for Cadna-owie Formation sandstone reservoirs.||||||12-JUL-16
19323|Wallumbilla Formation|69455|5|Briefly described|p39:4 Fig.39.3; 39:14-15|Early Cretaceous|Early Cretaceous|Provides a seal to Gilbert River Formation sandstone reservoirs in the offshore Western Gulf Sub-basin. Organic-rich shale is a possible source rock.||||||12-JUL-16
19323|Wallumbilla Formation|69457|3|Fully described|p41:2-3; 41:5 Fig.41.4; 41:6-10, 14-16|Early Cretaceous|Early Cretaceous|Vine et al. (1967). Eromanga, Carpentaria and Surat Basins. Mostly subsurface; outcrops form mesas, buttes or low rounded duricrusted hills. Shallow-marine, nearshore to marginal marine, minor non-marine deposits. 143m to over 350m thick. Equivalent to the succession comprising Bulldog Shale, Coorikiana Sandstone and lower part of Oodnadatta Formation. The name Bulldog Shale has previously (and inappropriately) been used to describe this Formation in the NT (eg Questa, 1990; Ambrose and Heugh, 2010). Has fair to occasionally excellent petroleum source intervals. May seal Cadna-owie Formation reservoirs.||Wilgunya Subgroup.|Doncaster, Coreena, Jones Valley, Ranmoor Members.|Overlies Cadna-owie Formation conformably, and Algebuckina Sandstone disconformably/unconformably. Is overlain conformably by Toolebuc Formation.|Mudstone and siltstone; minor thin intervals of fine sandstone and limestone. Locally calcareous, and may contain glauconite; shell fragments common in places. Locally silicified to porcellanite. Contains diverse fossil assemblages.|12-JUL-16
19323|Wallumbilla Formation|69582|5|Briefly described|p22, p25-p26, p29, p36, p65-p66|Lower Cretaceous|Lower Cretaceous|Eromanga and Surat basins. Deposited in a marine depositional environment. Intersected in GSQ Longreach 2 drillhole.||||Overlain by the Toolebuc Formation and the Surat Siltstone. Overlies the Bungil Formation and the Cadna-owie Formation.|Sandstone.|
19323|Wallumbilla Formation|69591|6|Mentioned|p101 Fig.2.96|||||||Overlies Gilbert River Formation. Is overlain by Toolebuc Formation.||
19323|Wallumbilla Formation|69594|4|Described|p518-519, p521-522, p526, p528-530, p534|Aptian|Barremian|See also p538, p540, p550, p573. Vine et al. (1967). Carpentaria, Eromanga, Laura and northern Surat Basins. Much of the upper part was previously known as Blackdown Formation (Laing and Power, 1959; Woods, 1961). Up to 475m thick. Contains a rich marine fauna (listed). Members not always discernible. RELATED UNITS (continued): Equivalent to Rolling Downs Group in the Laura Basin, the Roma Formation and lower part of overlying Tambo Formation.||Wilgunya Subgroup.|Coreena, Doncaster, Jones Valley, Ranmoor, Trimble Members.|Conformably overlies Gilbert River, Cadna-owie, Bungil Formations, Longsight Sandstone, Ronlow and Helby beds. Is overlain by Toolebuc Formation, Surat Siltstone and Allaru Mudstone. See COMMENTS.|Volcanogenic. Dominated by thick successions of sporadically nodular siltstone with lesser glauconitic sandstone, volcanic crystal-lithic sandstone and silty limestone.|
19323|Wallumbilla Formation|69673|5|Briefly described|p155 fig 127, p156, p159, p161|Cretaceous|Cretaceous|||Wilgunya Subgroup|Includes Doncaster Member, Coreena Member|Overlies Mount Anna Sandstone Member, Cadna-owie Formation overlain by Toolebuc Formation, correlated with Bulldog Shale|Mudstone, shale and siltstone with minor thin interbeds of fine sandstone and limestone.|
19323|Wallumbilla Formation|69681|6|Mentioned|p74 Fig.3, p82|Early Cretaceous|Early Cretaceous||||Includes Doncaster and Coreena Members.|||
19323|Wallumbilla Formation|69797|5|Briefly described|p17 Fig.2|Early Cretaceous|Early Cretaceous|Geol. Prov: Eromanga Basin.||||||
19323|Wallumbilla Formation|69946|3|Fully described|p19, p21-25, p56-57, p94|Early Cretaceous|Early Cretaceous|Vine et al. (1967); formerly Roma Formation, used by the petroleum industry. Type section is 'Wallumbilla Creek, from Wallumbilla Township south for 12 miles [19.3km]'. Distribution is by definition controlled by Toolebuc Formation: where absent, Bulldog Shale is used. Lithology is identical to Bulldog Shale. Up to 596m thick. Early Aptian-Albian. Wireline log correlations.||||Conformably overlies Cadna-owie Formation. Is overlain conformably by Toolebuc Formation.|Grey mudstone and siltstone with minor interbeds of fine-grained sandstone. Local pebbly and muddy diamictite containing metamorphic and sedimentary clasts.|
19323|Wallumbilla Formation|69947|5|Briefly described|p9, p13 Fig.7.2, p29 Fig.7.18|Early Cretaceous|Early Cretaceous|See also p31 Fig.7.20. Eromanga Basin.||Marree Subgroup.||Overlies Wyandra Sandstone Member (Cadna-owie Formation).|Thick, fossiliferous mudstones and siltstones.|
19323|Wallumbilla Formation|69948|6|Mentioned|p4; Figs.4.2, 18|||Eromanga Basin (an intracratonic basin). Sediment thickness, sonic log, gamma ray log all shown in contrast with Otway Basin (a rift basin).||||Overlies Cadna-owie Formation. Is overlain by Toolebuc Formation.|Marine shales.|
19323|Wallumbilla Formation|69952|5|Briefly described|p16|Cretaceous|Cretaceous|Eromanga Basin.||Unit in Rolling Downs Group.|||Mudstone, siltstone, sandstone; calcareous in part.|
19323|Wallumbilla Formation|70207|6|Mentioned|p14, p74|Early Cretaceous|Early Cretaceous|Georgetown region.||||||
19323|Wallumbilla Formation|70345|6|Mentioned|p3|Cretaceous|Cretaceous|||||||
19323|Wallumbilla Formation|70352|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|||Wilgunya Subgroup.|||Mudstone and siltstone with calcareous concretions.|
19323|Wallumbilla Formation|70354|5|Briefly described|Map legend|Cretaceous|Cretaceous|||Rolling Downs Group.||Is overlain by Toolebuc Formation.|Mudstone and siltstone with calcareous concretions.|
19323|Wallumbilla Formation|70572|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|||Wilgunya Subgroup|||Mudstone and siltstone with calcareous concretions.|20-JAN-22
19323|Wallumbilla Formation|70649|5|Briefly described|Map Legend|Cretaceous|Cretaceous|||Rolling Downs Group|Includes Coreena Member, Doncaster Member.||Marine grey mudstone and siltstone with minor interbeds of fine-grained glauconitic and calcareous sandstone, local thin micritic limestone beds and heavy mineral strandline accumulations; down-sequence glacial ice rafted erratics.|
19323|Wallumbilla Formation|70652|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Unconsolidated sediments also described.||Rolling Downs Group|Includes Coreena Member, Doncaster Member.|||
19323|Wallumbilla Formation|70673|6|Mentioned|p7|Cretaceous|Cretaceous|||||||
19323|Wallumbilla Formation|70720|6|Mentioned|p24-25|Early Cretaceous|Early Cretaceous||||Doncaster Member.|||
19323|Wallumbilla Formation|70821|4|Described|p21 Fig.2.6, p22 Fig.2.7, p23, p28|Early Cretaceous|Early Cretaceous|See also p30-31, p33, p79-80, p82, p85-88, p111-112, p117. Vine et al. (1967). The most widely distributed marine unit within the Great Australian Superbasin: Eromanga, Carpentaria, Laura and parts of Surat Basins. Varying thicknesses given from wells. Aptian to Albian age. Hydrochemistry mentioned; hydrostratigraphic properties. Equivalent to Bulldog Shale and Oodnadatta Formation.||Rolling Downs Group.|Doncaster, Coreena Members.|Overlies Cadna-owie and Bungil Formations, Hooray Sandstone and Drildool beds. Is overlain by Toolebuc Formation or Surat Siltstone; locally by Winton Formation (conformably).||
19323|Wallumbilla Formation|70823|5|Briefly described|p43-p44, p78|Early Cretaceous|Early Cretaceous|Eromanga Basin. Up to 450m thick. Deposited in open marine transgressive to regressive marine shoreface environments.||||Overlies the Cadna-owie Formation. Overlain by the Toolebuc Formation.||
19323|Wallumbilla Formation|70824|5|Briefly described|p9|Cretaceous|Cretaceous|Eromanga Basin.||||Overlies the Cadna-owie Formation. Overlain by the Toolebuc Formation.||
19323|Wallumbilla Formation|70836|6|Mentioned|p474|Early Cretaceous|Early Cretaceous|Lightning Ridge area, Surat Basin. Barremian-Albian.|||Coreena, Doncaster Members.|Overlies Bungil Formation. Is overlain by Surat Siltstone.||
19323|Wallumbilla Formation|70860|6|Mentioned|p281|||Great Artesian Basin.|||Coreena, Doncaster, Ranmoor, Jones Valley, Members.|||
19323|Wallumbilla Formation|71251|4|Described|p8, p11-13, p15, p17-20, p29|||First described by Isbell (1957). Eromanga Basin. 186m total thickness in Eulo 1 borehole; it was not possible to differentiate the two Members in this borehole. Natural gamma, magnetic susceptibility data tabulated. Conductivity data/diagram.||Rolling Downs Group.|Coreena and Doncaster Members.|Overlies Wyandra Sandstone Member (Cadna-owie Formation). Is overlain by Winton Formation.|Generally monotonous, glauconitic, marine, dark bluish-grey carbonaceous mudstone with some lignite plant fragments, some thin (estimated <1m) beds of siltstone and fine sandstone.|
19323|Wallumbilla Formation|71321|5|Briefly described|p15,27,65|Cenomanian|Cenomanian|Of Eromanga Basin. Previously known as Roma Formation. Regressivee depositional package following peak early Cretaceous marine transgression; marginal marine shoreface deposit.||||Equivalent to Bulldog Shale. Overlain by the Toolebuc Formation.||24-OCT-19
19323|Wallumbilla Formation|71342|3|Fully described|Ch4 p4, Ch4 p9, Ch4 p25|Albian|Aptian|Eromanga Basin. Formally defined by Vine et al (1967)  to replace the Roma Formation. Vine et al also defined the type section in "Wallumbilla Creek,from Wallumbilla Township south for 12 miles" in Queensland. This unit reaches a maximum thickness of 596m in Coonatie 1 in the Patchawarra Trough and 260m in the Poolowanna Trough. Age derived from palynology. Interpreted to have been deposited in a shallow epicontinental sea at cold high latitudes as debris flows. Spore-pollen zone is given in Ch5 p57. See also Ch5 p22, Ch5 p24-p25, Ch5 p30, Ch5 p57, Ch6 p8-p9, Ch7 p9, Ch7 p13, Ch10 p17, Ch11 p4-p5, Ch12 p12, Ch12 p14.||||Conformably overlies the Wyandra Sandstone Member (Cadna-owie Formation). Conformably overlain by the Toolebuc Formation.|Grey mudstone and siltstone with minor interbeds of fine-grained sandstone.|
19323|Wallumbilla Formation|71382|5|Briefly described|p4, p13, p16-p17, p19-p20|||Intersected in GSQ Julia 1 from 199.87m-310.49m for a total of 110.62m thickness. Temp log and stratlog are provided. Lithology is described in detail on p20. See also p23, p25, p27, App 3, 4.||||Overlies the Hooray Sandstone. Overlain by the Toolebuc Formation.|Interbedded mudstone and sandstone with minor calcareous mudstone.|
19323|Wallumbilla Formation|71855|4|Described|p2, p4-p6, p9-p10, p13|Jurassic|Jurassic|Eromanga and Carpentaria basins. In places the contact with the overlying Toolebuc Formation is disconformable or faulted. Wireline log responses were described for this unit including Gamma-ray, sonic transit time and resistivity. Structure is discussed. See also p15, p27, p33-p35, p50, p52-p53, p56-p57, p75.||||Conformably (gradationally) overlain by the Toolebuc Formation.|Glauconitic, smectite-rich mudstone, siltstone or fine-grained sandstone.|
19323|Wallumbilla Formation|71863|5|Briefly described|p4-p9|Albian|Aptian|Eromanga and Carpentaria basins. Deposited in a marine incursion.||Rolling Downs Group|Includes the Doncaster Member and the Coreena Member.|Overlies the Gilbert River Formation, Helby beds and the Cadna-owie Formation. Conformably overlain by the Toolebuc Formation.||
19323|Wallumbilla Formation|71864|4|Described|p8, p10, p13-p14, p16-p20|||Intersected in GSQ Eulo 2 borehole between 23-51m depth. Originally mapped in the area by Senior (1971). Described in Senior, 1971 as glauconitic marine siltstones and claystones. Gamma log characteristics and magnetic susceptibility is provided.||Rolling Downs Group|Includes the Coreena Member and the Doncaster Member.|Overlain by the Winton Formation. Overlies the Waihora Volcanics.|Dark blue to light grey siltstone with a distinctive layer producing carbonaceous flecks and a fine quartzose sandstone layer in addition to mudstone.|
19323|Wallumbilla Formation|71890|6|Mentioned|p7|||Surat Basin.||Rolling Downs Group||||
19323|Wallumbilla Formation|72297|5|Briefly described|p742, p746, p753|||Eromanga Basin. Acts as a regional seal. Potential hydrocarbon source rocks.|||Ranmoor Member.|Is overlain conformably by the Toolebuc Formation.|Shales and mudstones.|
19323|Wallumbilla Formation|72298|5|Briefly described|p801|Cretaceous|Cretaceous|Eromanga Basin (SA,QLD,NSW), Carpentaria Basin, Surat Basin (QLD,NSW), Coonamble Embayment (NSW).||Rolling Downs Group.|Doncaster, Coreena, Jones Valley, Ranmoor Members.|Overlies Wyandra Sandstone Member (Cadna-owie FZ); Gilbert River and Bungil FZs; Ronlow, Helby, Albany Pass and Drildool beds. Is overlain by Toolebuc FZ or Surat Siltstone.||
19323|Wallumbilla Formation|72913|6|Mentioned|p8.|||Two wells intersected this cover unit.||||||
19323|Wallumbilla Formation|72914|5|Briefly described|p12, p14, p16, p18, p20-21, p29, App. I|Cretaceous|Cretaceous|In Tongo 1 [borehole], the unit is semi-monotonous consisting chiefly of marine siltstone and claystone, but can occasionally has washes of coarser-grained quartzose sediments derived from local basement highs. Natural gamma emissions are relatively subdued and monotonous.||||Underlain by the Wyandra Sandstone Member (Cadna-owie Formation).|Marine siltstone and claystone with occasional washes of coarser-grained quartzose material.|
19323|Wallumbilla Formation|72915|6|Mentioned|p16, p19, p27, p39 App E, App I|Mesozoic|Mesozoic|Sedimentary rocks in the Congararra 1 borehole are attributed to the Rolling Downs Group, and may represent source-proximal Wallumbilla Formation (after Hawke and Cramsie, 1984). Mineralogical changes from clay-rich to quartz-rich are reflected in natural gamma emissions [data]. Relatively non-magnetic in Congararra 1. No groundwater was made from this unit in Congararra 1.||||||
19323|Wallumbilla Formation|72967|6|Mentioned|p5|||Carpenteria Basin.||Rolling Downs Group||||
19323|Wallumbilla Formation|72983|6|Mentioned|p15|Cretaceous|Cretaceous|||||||
19323|Wallumbilla Formation|73083|6|Mentioned|p62-63|Cretaceous|Cretaceous|||||Overlain by the Toolebuc Formation.|Mudstone and siltstone.|
19323|Wallumbilla Formation|73113|5|Briefly described|p. 22-24, 36-37, 41, 69, 80, 88, 116...|||Surat Basin. Tight aquitard. More locations: p. 119, 146, 151-152, 168-172, 177-178, 191.||||||
19323|Wallumbilla Formation|73137|6|Mentioned|p6, p81|Cretaceous|Cretaceous|Carpentaria Basin. Intersected in drill hole GIDPDS5.||||||08-OCT-22
19323|Wallumbilla Formation|73144|6|Mentioned|p8, p13|Cretaceous|Cretaceous|Carpentaria Basin. Leaky aquitard.||Rolling Downs Group||Underlain by Gilbert River Formation. Overlain by Toolebuc Formation.||
19323|Wallumbilla Formation|73147|5|Briefly described|p129|Aptian|Aptian|||Rolling Downs Group.||Overlies Gilbert River Formation. Is overlain by Toolebuc Formation.||
19323|Wallumbilla Formation|73167|6|Mentioned|p664 Fig. 2|Cretaceous|Cretaceous|Eromanga Basin.||||||
19323|Wallumbilla Formation|73203|6|Mentioned|p653|Early Cretaceous|Early Cretaceous||||Doncaster Member||Includes interbedded sandy/silty claystone and interbedded fine sandstones.|
19323|Wallumbilla Formation|73249|5|Briefly described|p319, p321, p323|Albian|Aptian|North and east of the Eromanga Basin [shown as within the Eromanga Basin on p319 Fig.2]. Laterally equivalent to the Bulldog Shale.||||Lateral equivalent to the Bulldog Shale, overlies the Cadna-owie Formation, underlies the Toolebuc Formation.|Siltstone and mudstone dominated.|
19323|Wallumbilla Formation|73251|6|Mentioned|p62|Early Cretaceous|Early Cretaceous|Eromanga Basin.||||Underlain by Wyandra Sandstone Member (Cadna-owie Formation). Overlain by Toolebuc Formation. Equivalent to Coorikiana Sandstone and Bulldog Shale.||
19323|Wallumbilla Formation|73281|6|Mentioned|p1, Appendix (DIP)|||Eromanga Basin. See DIP034_Petroleumdata.xlsx and DIP034_Welldata.xlsx.||||||
19323|Wallumbilla Formation|73343|6|Mentioned|p337|Cretaceous|Cretaceous|Eromanga Basin.||||Underlain by Wyandra Sandstone Member (Cadna-owie Formation). Overlain by Toolebuc Formation. Equivalent to Coorikiana Sandstone and Bulldog Shale.||
19323|Wallumbilla Formation|73472|6|Mentioned|p114|Cretaceous|Cretaceous|||||||
19323|Wallumbilla Formation|73479|5|Briefly described|p156 Fig.2, p159, p163, p164 Fig.7, p175|Cretaceous|Cretaceous|Eromanga Basin. Restricted open marine and shoreface depositional environment.|ca 125-104 Ma|||Overlies Wyandra Sandstone Member, underlies Toolebuc Formation||
19323|Wallumbilla Formation|73553|6|Mentioned|p7|Cretaceous|Cretaceous|||||||
19350|Wammerra Formation|22772|5|Briefly described|Table13.1|Cryogenian|Cryogenian|||||||
19350|Wammerra Formation|22857|5|Briefly described|Tb. 13.1 (insert p70-71)|Sturtian|Sturtian|Of the Eurowie Subgroup (Torrowangee Group). Lenticular flaggy limestone. Age: ~700Ma. Max. thickness: 750m. Geological Province: Adelaide Fold Belt. See also p398 App. 1 Tb.A1.3.||||||
19350|Wammerra Formation|30261|4|Described|Table 1|||Sturtian - Marinoan age.||||||
19350|Wammerra Formation|34812|3|Fully described|p82|||||||||
19350|Wammerra Formation|35199|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
19350|Wammerra Formation|36411|6|Mentioned|p270|||Refs Cooper et al. 1978 for definition.||||||
19350|Wammerra Formation|36733|6|Mentioned|Table 5|||||||||
19350|Wammerra Formation|37931|4|Described|p532|||||||||
19350|Wammerra Formation|39574|6|Mentioned|p155|||||||||
19350|Wammerra Formation|41405|5|Briefly described|p204|||||||||
19350|Wammerra Formation|70000|6|Mentioned|p34|Neoproterozoic|Neoproterozoic|||Unit in Euriowie Subgroup.||||
19350|Wammerra Formation|70015|5|Briefly described|Map legend|Cryogenian|Cryogenian|Mineral deposits (if any) are shown.||Unit in Euriowie Subgroup.||Is overlain by Tanyarto Formation.|Buff, flaggy, silty to sandy limestone grading into laminated siltstone-dominated sequences with minor limestone; thin, calcareous sandy interbeds common.|08-SEP-15
19366|Wandella Sandstone Member|2967|5|Briefly described|p46|||Referred to as Wandella Sandstone (see references p35, 46-47) except for this one mention as the current, formal Wandella Sandstone Member.||Parilla Sand.|||Contains heavy mineral bands.|
19366|Wandella Sandstone Member|10010|5|Briefly described|p12 Fig. 3|Late Pliocene|Early Pliocene|Of Loxton-Parilla Sand. Geological Province: Murray Basin.||||||13-AUG-07
19366|Wandella Sandstone Member|22773|5|Briefly described|Fig24.8p352|||||||||
19366|Wandella Sandstone Member|22799|5|Briefly described|p24 Fig.10|Early Pliocene|Early Pliocene|||||||
19366|Wandella Sandstone Member|22857|5|Briefly described|p352 Fig.24.8|Late Pliocene|Early Pliocene|Of the Parilla Sand? Geological Province: Murray Basin.||||||
19366|Wandella Sandstone Member|22887|5|Briefly described|Fig.6 p13|Late Pliocene|Early Pliocene|||||||
19366|Wandella Sandstone Member|22893|5|Briefly described|fig4 p9|||||||||
19366|Wandella Sandstone Member|23884|5|Briefly described|p155 Fig. 13.2|Pliocene|Pliocene|Geological Province: Murray Basin.||||||
19366|Wandella Sandstone Member|39329|6|Mentioned|p485|||See also Fig.1||||||
19366|Wandella Sandstone Member|40820|6|Mentioned|Fig.4|||||||||
19366|Wandella Sandstone Member|42130|6|Mentioned|Fig.3 P265|||||||||
19366|Wandella Sandstone Member|42134|6|Mentioned|Fig.3 P335|||||||||
19366|Wandella Sandstone Member|42966|2|Defined|Table 27, p172|Pliocene||of Loxton-Parilla Sands||||||
19366|Wandella Sandstone Member|43791|6|Mentioned|p372, Fig1|||||||||
19366|Wandella Sandstone Member|43804|6|Mentioned|Fig.2,p49|||||||||
19366|Wandella Sandstone Member|49040|6|Mentioned|Fig.6|||||||||
19366|Wandella Sandstone Member|65552|5|Briefly described|p5 Fig. 3|Late Pliocene|Early Pliocene|Of Loxton-Parilla Sands. Unconformably overlies Geera Clay and Olney Formation. Overlies Tragowel and Wandella Sandstone Members. Underlies Blanchetown Clay.||||||
19366|Wandella Sandstone Member|66286|6|Mentioned|p179, 188|||Southern Murray Basin. Regressive beach sequence.||Unit in Loxton-Parilla sands.||Overlies Tragowel Member.||
19366|Wandella Sandstone Member|72445|6|Mentioned|App.7 p7 Fig.4.|Pliocene|Miocene|Shown on the 'Lithostratigraphy of Cenozoic sediments in the Murray Basin' (from Brown & Stephenson 1991).||Probably of Loxton-Parilla Sands||May be partially equivalent to the Shepparton Formation, Wunghnu Group.|Shown as including sandstone.|
19406|Wangerrip Group|12796|6|Mentioned|p461|||Includes Massacre Shale.  Geological Province: Otway Basin||||||
19406|Wangerrip Group|22587|6|Mentioned|p79 Fig.7|Early Eocene|Late Paleocene|||||||
19406|Wangerrip Group|22674|5|Briefly described|p718, Fig.2 p719|Early Eocene|Maastrichtian|See also Fig.8 p725.||||||10-OCT-07
19406|Wangerrip Group|22875|4|Described|p13|Middle Eocene|Paleocene|In the Otway Basin.||||||10-OCT-07
19406|Wangerrip Group|22944|5|Briefly described|Fig3|Eocene|Paleocene|||||||
19406|Wangerrip Group|23230|4|Described|Table4-1p40, 41-3|Eocene|Paleocene|||||||
19406|Wangerrip Group|23307|5|Briefly described|Map Legend|Paleocene|Paleocene|||||||
19406|Wangerrip Group|23322|5|Briefly described|957 Fig.2|Eocene|Paleocene|Geological Province: Gambier Basin (SA) and Otway Basin (VIC).||||||07-SEP-09
19406|Wangerrip Group|23402|5|Briefly described|p31|Tertiary|Tertiary|Geological Province: Otway Basin.||||||21-OCT-08
19406|Wangerrip Group|23778|5|Briefly described|p660|||Geological Province: Otway Basin.||||||
19406|Wangerrip Group|23792|5|Briefly described|p26|Middle Eocene|Maastrichtian|Transgressive/regressive clastic cysles. Geological Province: Otway Basin.||||||
19406|Wangerrip Group|23939|6|Mentioned|Fig.5|||May be Paleocene to Early Eocene in age.||||||
19406|Wangerrip Group|24056|4|Described|p85|Paleocene|Paleocene|Geological Basin: Otway Basin.||||||
19406|Wangerrip Group|24200|5|Briefly described|p421, 422||Early Eocene|See also p423 Figs. 15 & 16, p428 Fig. 18.  Wangerrip Group Equivalents discussed throughout text.||||||
19406|Wangerrip Group|24202|5|Briefly described|p313 Fig. 2|Eocene|Paleocene|Geological Province: Gambier Sub-basin.  See also p312.||||||
19406|Wangerrip Group|24314|5|Briefly described|p61 Fig.2|Middle Eocene|Paleocene|Geological Province: Otway Basin. Max. Thickness 90m.||||||30-NOV-04
19406|Wangerrip Group|24323|5|Briefly described|p136 Fig. 3|Eocene|Paleocene|Overlies the Sherbrook Group. Overlain by the Nirranda Group. Geological Province: Otway Basin.||||||
19406|Wangerrip Group|24344|5|Briefly described|p69, 79|Paleocene|Paleocene|||||||
19406|Wangerrip Group|24470|6|Mentioned|p473|||||||||
19406|Wangerrip Group|24551|5|Briefly described|p246, 292 Fig. 10.3|Eocene|Late Cretaceous|Consists of: Pebble Point Formation, Pember Mudstone, Dilwyn Formation.||||||
19406|Wangerrip Group|24562|5|Briefly described|p7, 8, 35|Eocene|Paleocene|Overlies: Sherbrook Group (u). Geological Province: Otway Basin.||||||
19406|Wangerrip Group|29355|6|Mentioned|p179|||||||||
19406|Wangerrip Group|29823|5|Briefly described|p14|||||||||
19406|Wangerrip Group|29856|6|Mentioned|p40|||||||||
19406|Wangerrip Group|29889|6|Mentioned|p139|||||||||
19406|Wangerrip Group|30499|6|Mentioned|p92|||Stratigraphy||||||
19406|Wangerrip Group|30522|6|Mentioned|Map legend|Eocene|Paleocene|Eocene-Palaeocene||||||
19406|Wangerrip Group|30576|6|Mentioned|p23|||||||||
19406|Wangerrip Group|30578|4|Described|p8|||||||||
19406|Wangerrip Group|30580|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
19406|Wangerrip Group|30905|6|Mentioned|Table 7.4|||||||||
19406|Wangerrip Group|30928|6|Mentioned|Map legend|Paleocene|Paleocene|||||||
19406|Wangerrip Group|30932|6|Mentioned|Map legend|late Eocene|Paleocene|Equivalent Knight Group.U.Cret.? to Eocene?||||||
19406|Wangerrip Group|31036|1|Redefined|p195|early Tertiary|Late Cretaceous|See also p196-199, 215, Table 9-1. Late Cretaceous to Early Tertiary.||||||10-OCT-07
19406|Wangerrip Group|31245|5|Briefly described|p81|||Palaeocene. Formations listed.||||||10-OCT-07
19406|Wangerrip Group|31372|6|Mentioned|p9|||||||||
19406|Wangerrip Group|31424|6|Mentioned|Table 2|||Lithostratigraphy||||||
19406|Wangerrip Group|31534|6|Mentioned|p363|||See also Table 19-3||||||
19406|Wangerrip Group|31583|6|Mentioned|p18|||Section||||||
19406|Wangerrip Group|31624|6|Mentioned|p106|||U.Palaeocene flora||||||
19406|Wangerrip Group|31625|6|Mentioned|Fig. 5.2|||Palaeocene||||||
19406|Wangerrip Group|31920|5|Briefly described|p53|||See also p60. Palaeocene. Partly equivalent to Knight Group.||||||12-SEP-18
19406|Wangerrip Group|31922|6|Mentioned|p177|||||||||
19406|Wangerrip Group|32115|6|Mentioned|p1|||||||||
19406|Wangerrip Group|32117|6|Mentioned|Fig.2|||||||||
19406|Wangerrip Group|32162|6|Mentioned|p58|||See also Fig.5||||||
19406|Wangerrip Group|32898|6|Mentioned|Table 2-1|||||||||
19406|Wangerrip Group|33135|5|Briefly described|p17|||||||||
19406|Wangerrip Group|33949|6|Mentioned|p274|||||||||
19406|Wangerrip Group|34063|6|Mentioned|p2|||Paleocene. Table||||||
19406|Wangerrip Group|34164|6|Mentioned|p33|||Table.||||||
19406|Wangerrip Group|34343|5|Briefly described|p102|||||||||
19406|Wangerrip Group|34987|5|Briefly described|p170|||||||||
19406|Wangerrip Group|35013|6|Mentioned|p393|||||||||
19406|Wangerrip Group|35066|3|Fully described|p201|||||||||
19406|Wangerrip Group|35147|6|Mentioned|p127|||||||||
19406|Wangerrip Group|35285|5|Briefly described|p414|||||||||
19406|Wangerrip Group|36366|6|Mentioned|p1|||||||||
19406|Wangerrip Group|36913|6|Mentioned|Fig.4|||||||||
19406|Wangerrip Group|37548|6|Mentioned|p129|||||||||
19406|Wangerrip Group|38070|6|Mentioned|Fig.12|||Otway Basin||||||
19406|Wangerrip Group|38221|6|Mentioned|Fig.4|||Otway Basin||||||
19406|Wangerrip Group|38625|6|Mentioned|p271|||||||||
19406|Wangerrip Group|39315|6|Mentioned|Fig.7|||||||||
19406|Wangerrip Group|40003|5|Briefly described|p44|||See also Table 10.||||||10-OCT-07
19406|Wangerrip Group|40230|6|Mentioned|Fig.7|||||||||
19406|Wangerrip Group|40560|6|Mentioned|p4|||||||||
19406|Wangerrip Group|41016|5|Briefly described|Mention|||||||||
19406|Wangerrip Group|41185|5|Briefly described|p175|||||||||
19406|Wangerrip Group|41269|5|Briefly described|p246|||||||||
19406|Wangerrip Group|41487|5|Briefly described|p625|||||||||
19406|Wangerrip Group|41642|4|Described|p243|||See also Table 7.4||||||
19406|Wangerrip Group|41701|6|Mentioned|Map legend|early Eocene||||||||
19406|Wangerrip Group|41704|6|Mentioned|p100|||||||||
19406|Wangerrip Group|41714|6|Mentioned|p301|||||||||
19406|Wangerrip Group|41726|5|Briefly described|p421|||||||||
19406|Wangerrip Group|41769|4|Described|p18|||||||||
19406|Wangerrip Group|41868|5|Briefly described|p534|||||||||
19406|Wangerrip Group|42075|5|Briefly described|Fig.13 P252|||||||||
19406|Wangerrip Group|42318|6|Mentioned|p7|||||||||
19406|Wangerrip Group|42361|5|Briefly described|p18|||||||||
19406|Wangerrip Group|42453|6|Mentioned|p11|||||||||
19406|Wangerrip Group|42524|5|Briefly described|Fig.3 p27|||||||||12-SEP-18
19406|Wangerrip Group|42555|5|Briefly described|p285|||||||||
19406|Wangerrip Group|42599|5|Briefly described|Fig.3 P614|||||||||
19406|Wangerrip Group|42827|3|Fully described|p275|||see also Fig 8.10||||||
19406|Wangerrip Group|42863|5|Briefly described|Fig.14|||Variation on Victorian unit.||||||
19406|Wangerrip Group|43171|5|Briefly described|2-8|Middle Eocene|Paleogene|Within the Otway Supergroup.||||||07-NOV-08
19406|Wangerrip Group|43195|5|Briefly described|Map Legend|Eocene|Paleocene|See also commentary on back of map.||||||
19406|Wangerrip Group|43208|5|Briefly described|map legend||Maastrichtian|Of Maastrichian-Late Palaeocene age.||||||
19406|Wangerrip Group|43219|5|Briefly described|Fig.3,p6.|Eocene|Maastrichtian|||||||
19406|Wangerrip Group|43590|4|Described|p15|Tertiary|Late Cretaceous|||||||
19406|Wangerrip Group|43604|6|Mentioned|p144,Fig.1|Eocene|Paleocene|||||||
19406|Wangerrip Group|43660|6|Mentioned|Fig.6,p15||Tertiary|||||||
19406|Wangerrip Group|43733|6|Mentioned|Fig.2.11,p65||Tertiary|||||||
19406|Wangerrip Group|43744|6|Mentioned|Fig.3,p3|||||||||
19406|Wangerrip Group|43783|6|Mentioned|Fig14, p11|Middle Eocene|Paleocene|||||||
19406|Wangerrip Group|43784|6|Mentioned|Fig10, p12|Middle Eocene|Paleocene|||||||
19406|Wangerrip Group|43937|5|Briefly described|Map Legend|Paleocene|Santonian|||||||
19406|Wangerrip Group|44133|5|Briefly described|p154|Middle Eocene|Late Paleocene|Includes: Pebble Point Formation, Pember Mudstone, Dilwyn Formation. Geological Province: Gambier Basin.||||||
19406|Wangerrip Group|44135|6|Mentioned|p49|Early Eocene|Late Cretaceous|Mentioned in the context of correlates.||||||07-DEC-09
19406|Wangerrip Group|45159|6|Mentioned|p15|||||||||
19406|Wangerrip Group|45168|6|Mentioned|p6|||||||||
19406|Wangerrip Group|46802|6|Mentioned|Table 1|||||||||
19406|Wangerrip Group|48581|4|Described|p31|||See also p12,28,29,33,37,40, Fig.4,Pl.1,2. (J54-12/Port Cambell).||||||
19406|Wangerrip Group|48911|4|Described|p23|||Palaeocene - Middle Eocene.||||||21-OCT-08
19406|Wangerrip Group|48977|6|Mentioned|p2|||See also Table 3 & Fig.5||||||
19406|Wangerrip Group|49060|5|Briefly described|Fig.33 P53|||||||||
19406|Wangerrip Group|60421|5|Briefly described|p408 Fig. 1, 409|Eocene|Paleocene|Includes: Eastern View Formation.||||||07-NOV-08
19406|Wangerrip Group|60451|5|Briefly described|p95 Fig. 61|||||||||
19406|Wangerrip Group|60452|5|Briefly described|p14|Cenozoic|Cenozoic|Geological Province: Otway Basin.||||||19-NOV-08
19406|Wangerrip Group|60538|5|Briefly described|p470 Fig. 10, 473 Fig. 12|Early Eocene|Late Cretaceous|Mudstones, litoral deposits, sands and shales.||||||
19406|Wangerrip Group|60563|5|Briefly described|p45|Eocene|Paleocene|Overlain by the Nirranda Group. Geological Province: Otway Basin.||||||
19406|Wangerrip Group|60599|5|Briefly described|p84|Late Cretaceous|Late Cretaceous|Includes the Eastern View, Pebble Point and Wiridgil formations. Geological Province: Otway  Basin.||||||02-FEB-09
19406|Wangerrip Group|61017|5|Briefly described|p5 Fig. 2|Lutetian|Danian|Geological Province: Otway Basin.||||||07-FEB-11
19406|Wangerrip Group|61180|5|Briefly described|p33|Tertiary|Tertiary|Contains phosphate deposits.  Age is Early Tertiary. Geological Province: Otway Basin.||||||
19406|Wangerrip Group|61182|3|Fully described|p19, p35|Early Eocene|Paleocene|Incl: Pebble Point and Dilwyn Fms; some include Sherbrook Gp rocks. Moomowroong Sand and Wiridjil Gravel have been added as they grade into Pebble Point Fm and each other. Unconformable on Sherbrook Gp. Overlain by Nirranda Gp. Otway Basin. Age: 65-45Ma.||||||06-JAN-10
19406|Wangerrip Group|61185|5|Briefly described|p57|Tertiary|Tertiary|Includes Pebble Point Formation, Wiridgil Formation and Eastern View Formation (Edwards et al. 1996). Equivalent to White Hills Gravel and Warina Sand. Age: ~65Ma. Geol. Prov: Otway Basin.||||||07-FEB-11
19406|Wangerrip Group|61470|5|Briefly described|p28 Fig. 5|Lutetian|Danian|Includes Pebble Point formation, Pember Mudstone and Dilwyn Formation. Geological Province: Otway Basin.||||||12-OCT-05
19406|Wangerrip Group|61528|6|Mentioned|p827|||||||||
19406|Wangerrip Group|61547|5|Briefly described|p461 Fig.2, p462. |Eocene|Paleocene||||Includes basal Pebble Point Formation, Pember Mudstone and Dilwyn Formation.|Unconformably overlies Sherbrook Group. Is overlain by Nirranda Group.||05-FEB-15
19406|Wangerrip Group|61607|6|Mentioned|p5 Fig. 2|Eocene|Paleocene|Geological Province: Otway Basin.||||||12-MAR-09
19406|Wangerrip Group|61608|6|Mentioned|p41 Fig. 5|||Refers to equivalent unit.||||||
19406|Wangerrip Group|61622|4|Described|p436, p437, p436 Fig. 2|Early Tertiary|Late Cretaceous|Includes Pebble Point Fm, Pember Mudst and Dilwyn Fm. Thickness: 200m. Geological Province: Otway Basin. Thin oolitic deposits and a range of mudstones and sandstones.||||||07-FEB-11
19406|Wangerrip Group|61623|5|Briefly described|p447, p449 Fig. 4|Tertiary|Tertiary|Includes Pebble Point Formation, Pember Mudstone and Dilwyn Formation. Geological Province: Otway Basin.||||||
19406|Wangerrip Group|61624|6|Mentioned|p465|Tertiary|Tertiary|Geological Province: Otway Basin.||||||07-APR-09
19406|Wangerrip Group|61626|5|Briefly described|p486, p487, p486 Fig. 2, p488, p493|Eocene|Paleocene|Includes; Pebble Point and Dilwyn Fomations and Pember Mudstone. Geological Province: Otway Basin.||||||07-APR-09
19406|Wangerrip Group|61627|5|Briefly described|p500 Fig. 2|Eocene|Paleocene|Includes Dilwyn and Pebble Point Formations, Pember Mudstone. Geological Province: Otway Basin.||||||07-FEB-11
19406|Wangerrip Group|61628|5|Briefly described|p509 Fig. 3|Middle Eocene|Late Cretaceous|Includes; Pebble Point and Dilwyn Formations, Pember Mudstone. Geological Province: Otway Basin.||||||
19406|Wangerrip Group|61841|5|Briefly described|p242|Eocene|Paleocene|Shallow marine to continental deposits.   Geological Province: Otway Basin.||||||03-JUL-06
19406|Wangerrip Group|62370|6|Mentioned|p455, p461|||Siliclastic sediments. Geological Province: Otway Basin.||||||
19406|Wangerrip Group|62896|5|Briefly described|p87|||Geological Province: Otway Basin.||||||07-FEB-11
19406|Wangerrip Group|63122|5|Briefly described|p17 Fig. 4.3, p21|Eocene|Early Paleocene|Includes Pebble Point Formation, Pember Mudstone and Dilwyn Formation. Geological Province: Otway Basin.||||||
19406|Wangerrip Group|63124|5|Briefly described|p49 Fig. 5.2, p87 Fig. 5.29, p84|Middle Eocene|Early Paleocene|Includes Pebble Point and Dilwyn Formations, and Pember Mudstone. Geological Province: Otway Basin.||||||
19406|Wangerrip Group|63125|6|Mentioned|p115|||Geological Province: Otway Basin||||||
19406|Wangerrip Group|63173|5|Briefly described|p342 Fig. 9.2|Middle Eocene|Early Paleocene|Geological Province: Otway Basin, offshore.||||||07-FEB-11
19406|Wangerrip Group|63269|5|Briefly described|p604-605|Eocene|Late Cretaceous|Otway Basin.|||Eastern View, Pebble Point, Dilwyn Formations; Pember Mudstone.|Unconformably overlies Sherbrook Group. Is overlain unconformably by Nirranda Group.||
19406|Wangerrip Group|63431|5|Briefly described|p677 Fig. 2|Eocene|Paleocene|Includes the Pebble point Formation, Pember Mudstone and Dilwyn Formation. Overlies the Sherbrook Group; Geological Province: Penola Trough/Otway Basin.||||||07-FEB-11
19406|Wangerrip Group|63446|5|Briefly described|Map legend|Paleocene|Paleocene||||||Marine, fluvial: sandstone, minor conglomerate.|
19406|Wangerrip Group|63740|5|Briefly described|p88|Early Eocene|Late Paleocene|Includes Dilwyn Formation. Geological province: Otway Basin.||||||07-FEB-11
19406|Wangerrip Group|64314|5|Briefly described|p504|Early Eocene|Paleocene|Unconformably overlies Sherbrook Group.||||||21-OCT-08
19406|Wangerrip Group|65715|5|Briefly described|p11 Tb.7|Paleogene|Paleogene|Includes Dilwyn Formation, Moomowroong Sand and Wiridjil Gravel.||||||
19406|Wangerrip Group|66002|4|Described|p3, p10 Tb.7, p10 Tb.8, p11|Paleogene|Paleogene|Includes Dilwyn Formation, Moomowroong Sand, Wiridjil Gravel and Pebble Point Formation. Outcrops extensively in the Port Campbell Embayment. Overlies Eumeralla Formation. Newly subdivided in this paper||||||
19406|Wangerrip Group|66012|5|Briefly described|p17|||In Otway Basin. Carbonaceous-rich. Correlated with Dilwyn Formation? or includes Dilwyn Formation.|| ||||16-FEB-15
19406|Wangerrip Group|66181|6|Mentioned|p312|Eocene||Gippsland Basin||||||
19406|Wangerrip Group|66245|5|Briefly described|p6 Fig.5, p8, p27 Fig.32. |Lutetian|Maastrichtian|Coastal and shallow marine, progradational sequence of clastic sediments.|||Includes Pebble Point, Dilwyn and ?Eastern View Formations and Pember Mudstone.|||
19406|Wangerrip Group|67061|6|Mentioned|p545, p546 Fig.3.|Eocene|Paleocene|Equivalent to upper parts of Eastern View Group (Torquay Sub-basin).|||Includes Pebble Point Formation, Pember Mudstone and Dilwyn Formation.|||
19406|Wangerrip Group|67366|5|Briefly described|p103 Fig.2. |Eocene|Paleocene||||Includes basal Massacre Shale; Pebble Point Formation; Pember Mudstone, and Dilwyn Formation at the top.|Unconformably overlies Sherbrook Group. Is unconformably overlain by Nirranda Group.||05-FEB-15
19406|Wangerrip Group|67367|5|Briefly described|p130, p131 Fig.2. |Lutetian|Maastrichtian|Siliciclastics. Stratigraphic equivalent to Latrobe Group, offshore Gippsland Basin.|||Includes Massacre Shale, Pebble Point and Dilwyn Formations, and Pember Mudstone.|||
19406|Wangerrip Group|68116|5|Briefly described|Appendix, Map 38.|Eocene|Paleocene||||||Silty clay, clayey silt, fine quartz sand: carbonaceous, micaceous, pyritic, burrowed, with abundant arenaceous foraminifers, minor calcareous foraminifers and shelly fossils; shallow marine (below and close to storm wave base) deposits.|
19406|Wangerrip Group|69297|6|Mentioned|p78, p79, p98, p112, p115, p116|Lutetian|Maastrichtian|Otway and Sorell Basins. Coastal plain to open marine siliciclastic and carbonate sediments. Potential reservoir in the Sorell Basin. May contain intraformational shale seals.|||Includes the Wiridjil Gravel, Massacre Shale, Pebble Point Formation, Pember Mudstone and the Dilwyn Formation.|Overlies the Sherbrook Group. Unconformably overlain by the Nirranda Group.||
19406|Wangerrip Group|69651|5|Briefly described|p6, p10, p12, p28, p32-35, p38|Eocene|Paleocene|Otway Basin. Coastal plain, deltaic and inner shelf deposits. Has fault/stratigraphic traps and stratigraphic reservoirs. Very high (30%+) porosity values. Modelling diagrams.|||Eastern View, Pebble Point, Dilwyn Formations; Pember Mudstone.|Unconformably overlies Sherbrook Group. Is overlain unconformably by Nirranda Group.|Includes interbedded sandstones.|
19406|Wangerrip Group|69879|5|Briefly described|p418, p424|Eocene|Maastrichtian|Strahan Sub-basin. Shown as Wangerrip Group equivalent. Offshore exploration well Cape Sorell 1.||||Overlies Sherbrook Group. Underlies Nirranda Group.|Alternating beds of silty claystone/clayey siltstone (with organic content and terrestrial input) with clastics, and quartzitic sandstone. Shallow marine quartz sandstone, siltstone and mudstone.|
19406|Wangerrip Group|70077|5|Briefly described|Nelson: Fig.2. Regional: Fig.4; p5, p7|Eocene|Maastrichtian|Otway Basin: Gambier Embayment and Voluta Trough. May be petroleum sources of the Austral 3 Petroleum System.|||Massacre Shale; Pebble Point and Dilwyn Formations; Pember Mudstone; Wiridjil Gravel.|Overlies Sherbrook Group. Is overlain by Nirranda Group.||
19406|Wangerrip Group|70078|5|Briefly described|Northern:Fig.2; p2. Regional:Fig.4; p5-6|Eocene|Late Cretaceous|Otway Basin. Sandstones equivalent to this unit in the Sorell Basin are potential hydrocarbon sources; sealed by Heytesbury Group marls and fine-grained carbonates.|||Massacre Shale; Pebble Point and Dilwyn Formations; Pember Mudstone.|Overlies Sherbrook Group. Is overlain by Nirranda Group.||
19406|Wangerrip Group|70379|5|Briefly described|p723-727, p732|Eocene|Eocene|Otway Basin.||||Overlies Sherbrook Group or (locally) Eumeralla Formation. Is overlain by Nirranda Group.||
19406|Wangerrip Group|71419|6|Mentioned|p16 Fig 17|Eocene|Paleocene|Fluvial sediments.||||||
19406|Wangerrip Group|71437|4|Described|Fig. 1 opp p154, p153, p159|Eocene|Albian|Here redefined to embrace Upper Cretaceous as well as lower Tertiary sediments (Cycles 1 and 2).|||Includes Waarre Sandstone, Flaxman Formation, Paaratte Formation, Pebble Point Formation, Dilwyn Formation.|Overlain by Nirranda Group.|Sands, shales, siltstones, and mudstones with minor dolomites, siderite-ankerite, coal, gravels, and greensands.|
19406|Wangerrip Group|71593|5|Briefly described|p51|Eocene|Cretaceous|||||||
19406|Wangerrip Group|73356|6|Mentioned|p3, p15-16|||Transgressive siliciclastics. Reaches a maximum thickness of more than 1200 m in the Portland Trough.||||||
19406|Wangerrip Group|73357|6|Mentioned|p44, p46, p48|Bartonian|Danian|Otway Basin.|||Includes K/Pg Boundary Shale, Pebble Point Formation, Pember Mudstone, Dilwyn Formation.|Underlies Nirranda Group.||
19406|Wangerrip Group|73383|4|Described|p3, p7 Tb.3.1, p10, p21, p27|Eocene|Maastrichtian|Otway Basin. Paleocene to mid Eocene. Equivalent to chemostratigraphic Sequence S5 which has generally lower Ti/Th values than other sequences in Otway Basin. Includes high Fe and P intervals, likely related to berthierine 'greensands'.|||Pebble Point Formation, Pember Mudstone, Dilwyn Formation|Overlies Sherbrook Group, underlies Nirranda Group|Clastic units including sandstones and mudstones.|
19406|Wangerrip Group|73385|5|Briefly described|p3-5, p23-24|Eocene|Maastrichtian|Otway Basin. Maximum thickness of more than 1200 m in the Portland Trough, thins across the Bridgewater High. Deposited in basin margin subsidence event.|||Pebble Point Formation, Pember Mudstone, Dilwyn Formation|Overlies Sherbrook Group, unconformably underlies Nirranda Group.|Transgressive siliciclastic group.|
19406|Wangerrip Group|73386|4|Described|p1-2, p4-7, p10, p12-13, Attachment A1|Eocene|Maastrichtian|Otway Basin. Represents transition from active rifting to post-rifting subsidence. Progradational, overlies a regional intra-Maastrichtian unconformity and onlaps the top of the Otway Group, underlies intra-Lutetian unconformity. Thickest offshore, maximum thickness of over 1200 m in the Portland Trough, thins to the northeast. Latest Cretaceous to mid Eocene age, Upper Forcipites longus to Lower Nothofagidites asperus spore-pollen zones, chemostratigraphic sequence S5 of Forbes et al. (2020). Location in text includes iii.|||Dilwyn Formation, Pember Mudstone, Pebble Point Formation, Cretaceous/Paleogene boundary shale|Unconformably overlies Sherbrook Group, unconformably underlies Nirranda Group|Siliciclastic sandstones, mudstones, siltstone and shale.|
19406|Wangerrip Group|73594|5|Briefly described|p4-5|Eocene|Paleocene|Otway Basin. Characterised by a series of propagating delta systems, maximum thickness of 2200m in the Portland Trough.|||Pebble Point Formation, Pember Mudstone, Dilwyn Formation|Overlies Sherbrook Group, underlies Nirranda Group||
19410|Wangkonda Formation|9124|6|Mentioned|Map Legend|Cambrian|Cambrian|||||||
19410|Wangkonda Formation|22643|5|Briefly described|fig3p187|Early Cambrian|Early Cambrian|||||||
19410|Wangkonda Formation|22766|4|Described|Fig.2 p561, p562||Tommotian|||||||
19410|Wangkonda Formation|23827|6|Mentioned|p260 Fig.3|||||||||
19410|Wangkonda Formation|23981|5|Briefly described|p8-9 Fig. 4, p10 Fig. 5|Early Cambrian|Early Cambrian|Conformably overlies Mount Terrible Formation; conformably underlies Sellick Hill Formation. Max. thickness: 110m. Geological Province: Stansbury Basin (Fleurieu Pen.) Oolitic grainstone, fenstral limestone with 'bird eye' structures, and thrombolites.||||||04-FEB-08
19410|Wangkonda Formation|24465|6|Mentioned|p358|Early Cambrian|Early Cambrian|Of Normanville Group.  Geological Province: Stansbury Basin.||||||19-JAN-05
19410|Wangkonda Formation|33332|6|Mentioned|p11|||L.Camb.||||||
19410|Wangkonda Formation|35255|6|Mentioned|Fig.8|||||||||
19410|Wangkonda Formation|38873|6|Mentioned|Table 2|||||||||
19410|Wangkonda Formation|39806|6|Mentioned|p207|||||||||
19410|Wangkonda Formation|40442|5|Briefly described|p13|||||||||
19410|Wangkonda Formation|40455|5|Briefly described|p67|||||||||
19410|Wangkonda Formation|40852|6|Mentioned|p32|||||||||
19410|Wangkonda Formation|41103|6|Mentioned|Fig.1|||||||||
19410|Wangkonda Formation|41526|6|Mentioned|p61|||||||||
19410|Wangkonda Formation|42222|6|Mentioned|Table 1 P4|||||||||
19410|Wangkonda Formation|42225|6|Mentioned|Fig.4 P224|||||||||
19410|Wangkonda Formation|42232|4|Described|p283|||||||||
19410|Wangkonda Formation|42266|5|Briefly described|p291|||||||||
19410|Wangkonda Formation|42268|6|Mentioned|p329|||||||||
19410|Wangkonda Formation|42270|6|Mentioned|p353|||||||||
19410|Wangkonda Formation|42488|5|Briefly described|Fig.2 P187|||||||||
19410|Wangkonda Formation|43703|6|Mentioned|Fig.1,p75|||||||||
19410|Wangkonda Formation|44133|5|Briefly described|p4 Fig. 7.2, 6, 8|Early Cambrian|Early Cambrian|Geological Province: Stansbury Basin. Of the Normanville Group.||||||
19410|Wangkonda Formation|60712|5|Briefly described|p28 Fig. 1|Early Cambrian|Early Cambrian|Of the Normanville Group.||||||
19410|Wangkonda Formation|61307|5|Briefly described|p6 Fig. 3|Cambrian|Cambrian|Of the Normanville Group. Geological Province: Adelaide Fold Belt.||||||
19410|Wangkonda Formation|63848|6|Mentioned|p534 Fig.4.|||||Unit in Normanville Group.||Overlies Mount Terrible Formation. Is overlain by Sellick Hill Formation.||
19410|Wangkonda Formation|64282|5|Briefly described|Map legend|Early Cambrian|Early Cambrian|Coarse-grained impure marble on Dudley Peninsula. In the Stansbury Basin this unit comprises bioturbated calcareous sandstone, glauconitic sandstone and mottled, muddy limestone.||||||02-JUL-08
19410|Wangkonda Formation|65375|5|Briefly described|p33.|Early Cambrian|Early Cambrian|||Unit in Normanville Group.||Overlies Mount Terrible Formation. Is overlain by Sellick Hill Formation.||
19410|Wangkonda Formation|65892|5|Briefly described|p9 Fig.4, p14-16. |Early Cambrian|Early Cambrian|Fleurieu Peninsula. 110m thick. Peritidal, carbonate-dominated mudflats and stream channel deposits.||Unit in Normanville Group.||Conformably overlies Mount Terrible Formation. Is overlain disconformably by Sellick Hill Formation.|Stromatolitic, intraclastic and fenestral micritic limestone with ooid grainstone.|
19410|Wangkonda Formation|66761|5|Briefly described|p244, 246, 254|Cambrian|Cambrian|16 m interval in PIRSA stratigraphic hole Investigator 1. Better known from Fleurieu Peninsula.||||Overlies Winulta Formation,? Mount Terrible Formation; overlain by Parara Limestone.||14-MAR-12
19410|Wangkonda Formation|68735|5|Briefly described|p233 Fig.2, p235 Fig.3|Early Cambrian|Early Cambrian|Stansbury Basin.||Of the Normanville Group.||||
19410|Wangkonda Formation|68993|6|Mentioned|p544 Fig.1|Early Cambrian|Early Cambrian|Fleurieu Peninsula.||Of the Normanville Group.||||
19410|Wangkonda Formation|70833|5|Briefly described|p200|Cambrian|Cambrian|Of Eastern Stansbury Basin.||||Overlain by Sellick Hill Formation. Underlain unconformably by Mount Terrible Formation.||
19410|Wangkonda Formation|72450|5|Briefly described|Brochure map||||c. 520 Ma|Normanville Group|||Massive, dark grey limestone.|
19410|Wangkonda Formation|73107|5|Briefly described|Map legend.|Early Cambrian|Early Cambrian|Dudley Peninsula.|||||Coarse-grained impure marble (Dudley Peninsula). Bioturbated calcareous sandstone, glauconitic sandstone and mottled muddy limestone (Stansbury Basin).|
19410|Wangkonda Formation|73188|6|Mentioned|p316|Early Cambrian|Early Cambrian|Mount Lofty Ranges.||Normanville Group|||Limestone, calcareous sandstone.|
19410|Wangkonda Formation|73247|6|Mentioned|p205|Cambrian (Stage 2)|Cambrian (Stage 2)|"Fleurieu Peninsula. [Also written as ""Wangkonda Formation"" in the Kangaroo Island Investigator 1 Big Gully section; inferred to indicate tentative correlation]."||||Underlain by Mount Terrible Formation. Unconformably overlain by Sellick Hill Formation.||
19426|Wantapella Volcanics|22746|5|Briefly described|Fig.3 p515|Cryogenian|Cryogenian|||||||
19426|Wantapella Volcanics|22804|6|Mentioned|p443|||||||||
19426|Wantapella Volcanics|22922|5|Briefly described|33|Neoproterozoic|Neoproterozoic|Sturtian age.||||||
19426|Wantapella Volcanics|23282|2|Defined|p56||Neoproterozoic|Age: Precambrian, Neoproterozoic, either late Sturtian or early Marinoan Epochs. of Krieg (1973) and later by Preiss (1993).||||||
19426|Wantapella Volcanics|23288|6|Mentioned|p129 Fig.5|||of Central and Eastern Officer Basin.||||||
19426|Wantapella Volcanics|24067|5|Briefly described|p249 Fig.2|Adelaidean|Adelaidean|Geological Province: Officer Basin.||||||
19426|Wantapella Volcanics|24112|5|Briefly described|p254 Fig.2|Neoproterozoic|Neoproterozoic|Geological Province: Officer Basin.||||||16-SEP-08
19426|Wantapella Volcanics|30807|6|Mentioned|p102|||Suggested map symbol.||||||16-SEP-08
19426|Wantapella Volcanics|31698|6|Mentioned|Map legend|Precambrian|Precambrian|Sturtian||||||
19426|Wantapella Volcanics|35628|4|Described|Table 2|||||||||
19426|Wantapella Volcanics|36096|6|Mentioned|Fig.3|||||||||
19426|Wantapella Volcanics|36920|6|Mentioned|p168|||||||||
19426|Wantapella Volcanics|38157|6|Mentioned|Table VIII|||||||||
19426|Wantapella Volcanics|39352|6|Mentioned|Map legend|Precambrian|Precambrian|Sturtian||||||
19426|Wantapella Volcanics|40910|6|Mentioned|p11|||||||||
19426|Wantapella Volcanics|40945|6|Mentioned|Fig.3|||||||||
19426|Wantapella Volcanics|41405|3|Fully described|p202|||||||||
19426|Wantapella Volcanics|42246|6|Mentioned|p16|||||||||
19426|Wantapella Volcanics|43052|5|Briefly described|p199,Table 6.2|||||||||
19426|Wantapella Volcanics|43743|6|Mentioned|Fig.2,p33||Neoproterozoic|||||||
19426|Wantapella Volcanics|49792|5|Briefly described|Fig.5|||||||||
19426|Wantapella Volcanics|50327|6|Mentioned|p309|||Basaltic volcanics in the interior of the Australia cration.||||||07-FEB-11
19426|Wantapella Volcanics|60953|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Basalt.||||||
19426|Wantapella Volcanics|61108|5|Briefly described|map legend|Adelaidean|Adelaidean|Basalt. Age and correlation very uncertain.||||||06-JUN-05
19426|Wantapella Volcanics|61732|5|Briefly described|p4 Fig. 3, p58 Fig. 22|Sturtian|Sturtian|?Of Lake Maurice Group? Geological Province: eastern and central Officer Basin. See also p145 Fig. 51.||||||07-FEB-11
19426|Wantapella Volcanics|62453|5|Briefly described|p12 Fig. 8|Cryogenian|Cryogenian|Geological Province: Officer Basin.||||||
19426|Wantapella Volcanics|63397|6|Mentioned|p5|Neoproterozoic|Neoproterozoic|||||||18-JUL-07
19426|Wantapella Volcanics|64794|6|Mentioned|p238 fig 2|Cryogenian|Cryogenian|||||||
19426|Wantapella Volcanics|64970|6|Mentioned|p719 Fig. 2|Sturtian|Sturtian|Geological Province: Officer Basin.||||||27-MAY-09
19426|Wantapella Volcanics|65365|5|Briefly described|p10 Fig. 4|Cryogenian|Cryogenian|Eastern Officer Basin||||||
19426|Wantapella Volcanics|65366|5|Briefly described|p23 Fig. 3|Cryogenian|Cryogenian|Eastern Officer Basin||||||
19426|Wantapella Volcanics|65376|6|Mentioned|p247 Fig.6.57.|Neoproterozoic|Neoproterozoic|||||||
19426|Wantapella Volcanics|67120|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic||||||Basalt, altered, amygdaloidal, tholeiitic; with lithic and gritty sandstone interbeds.|
19426|Wantapella Volcanics|67536|6|Mentioned|Map Legend||||||||Basalt.|
19426|Wantapella Volcanics|68270|5|Briefly described|p678,683|Cryogenian|Cryogenian|Eastern Officer Basin.||||Underlain unconformably by Chambers Bluff Tillite.||
19426|Wantapella Volcanics|70336|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic||||||Altered amygdaloidal tholeiitic basalt, with lithic and gritty sandstone interbeds.|
19426|Wantapella Volcanics|72478|6|Mentioned|p8|Sturtian|Sturtian|Officer Basin.|c. 700 Ma|||Unconformably overlies the Chambers Bluff Tillite.Unconformably overlain by Lake Maurice Group.||24-MAR-21
19426|Wantapella Volcanics|73090|5|Briefly described|Appendix.|Neoproterozoic|Neoproterozoic||||||Basalt, altered, amygdaloidal, tholeiitic; with lithic and gritty sandstone interbeds.|
19462|Warina Sand|2967|5|Briefly described|p14, p15 Fig.2.2, p17, 20, 77, 336|||Lawrence (1975). This unit is the basal regional aquifer in the Murray Basin. Lower Tertiary.||Renmark Group.||Is overlain by Olney Formation.|Medium- to coarse-grained quartz sand, sparingly carbonaceous and pyritic. Lesser gravel, ligneous clays and silts, minor lignites.|
19462|Warina Sand|10010|5|Briefly described|p12 Fig. 3|Early Eocene|Late Paleocene|Of the Renmark Group. Geological Province: Murray Basin.||||||13-AUG-07
19462|Warina Sand|22495|6|Mentioned|P222|||||||||
19462|Warina Sand|22587|6|Mentioned|p79 Fig.7|Middle Eocene|Middle Eocene|||||||
19462|Warina Sand|22712|5|Briefly described|p132|Tertiary|Tertiary|Of the Renmark Group.||||||15-JAN-09
19462|Warina Sand|22773|5|Briefly described|p351,Fig24.8p352|Early Eocene|Late Paleocene|||||||
19462|Warina Sand|22799|3|Fully described|p27|Middle Eocene|Early Eocene|||||||
19462|Warina Sand|22857|5|Briefly described|p351, p352 Fig. 24.8|Eocene|Late Paleocene|Basal unit of the Renmark Group. Overlain by Olney Formation. Age: ~60Ma. Max. thickness: ~200m. Geological Province: Murray Basin. See also p353 Fig. 24.9.||||||
19462|Warina Sand|22887|5|Briefly described|Fig.6|Early Eocene|Late Paleocene|||||||
19462|Warina Sand|22893|5|Briefly described|fig4 p9|||||||||
19462|Warina Sand|23884|5|Briefly described|p153, p155 Fig. 13.2|Early Eocene|Late Paleozoic|Geological Province: Murray Basin. Age: ~60 Ma. Of the Renmark Group.||||||07-NOV-08
19462|Warina Sand|24105|5|Briefly described|p155|Eocene|Paleocene|Geological Province: Murray Basin. Overlying Unit: Olney Formation.||||||
19462|Warina Sand|24177|5|Briefly described|p69, p70|Paleogene|Paleogene|Of the Renmark Group. Overlain by Olney Formation. Age: <65 Ma. Geological Province: Murray Basin.||||||07-NOV-08
19462|Warina Sand|24551|6|Mentioned|p320, 421, 731 Table 17.1|||Of the Renmark Group. Maximum Thickness: 200m.||||||
19462|Warina Sand|30581|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
19462|Warina Sand|30934|6|Mentioned|Map legend|Eocene|Eocene|||||||
19462|Warina Sand|31741|6|Mentioned|p6|||||||||
19462|Warina Sand|31745|6|Mentioned|Map legend|Eocene|Eocene|||||||
19462|Warina Sand|31746|4|Described|p193|||||||||
19462|Warina Sand|34757|6|Mentioned|p45|||||||||
19462|Warina Sand|34813|5|Briefly described|p63|||Mention on P62 also.||||||
19462|Warina Sand|37809|6|Mentioned|Fig.7|||||||||
19462|Warina Sand|37873|6|Mentioned|p1|||||||||
19462|Warina Sand|38601|5|Briefly described|p7|||||||||
19462|Warina Sand|39329|6|Mentioned|Fig.1|||||||||
19462|Warina Sand|39929|6|Mentioned|p269|||||||||
19462|Warina Sand|41136|5|Briefly described|p215|||||||||
19462|Warina Sand|41868|5|Briefly described|p551|||||||||
19462|Warina Sand|42125|5|Briefly described|p132|||See also p139.||||||15-JAN-09
19462|Warina Sand|42126|6|Mentioned|p156, p149|||||||||
19462|Warina Sand|42130|6|Mentioned|Fig.3 p265|||||||||03-DEC-13
19462|Warina Sand|42133|6|Mentioned|p302|||||||||
19462|Warina Sand|42137|6|Mentioned|Fig.2 P368|||||||||
19462|Warina Sand|42138|6|Mentioned|p389|||||||||
19462|Warina Sand|42184|6|Mentioned|Fig.2 P348|||||||||
19462|Warina Sand|42720|6|Mentioned|map legend|Oligocene|Paleocene|||||||
19462|Warina Sand|42813|6|Mentioned|p24|||||||||
19462|Warina Sand|42827|5|Briefly described|p267|||Of Renmark Group.||||||27-OCT-08
19462|Warina Sand|42881|4|Described|Fig.3, P84|||||||||
19462|Warina Sand|42966|2|Defined|p97|Eocene|Paleocene|Of Renmark Group.||||||13-AUG-07
19462|Warina Sand|43052|5|Briefly described|Table 2.1|||||||||
19462|Warina Sand|43218|4|Described|Fig.3,p22||Tertiary|Of the Renmark Group.||||||27-OCT-08
19462|Warina Sand|43780|5|Briefly described|p6|Eocene|Paleocene|||||||
19462|Warina Sand|43791|6|Mentioned|p372, Fig1|||||||||
19462|Warina Sand|43804|6|Mentioned|Fig.2,p49|||||||||
19462|Warina Sand|44093|5|Briefly described|p145 App. 1|Tertiary|Tertiary|Geological Province: Kanmantoo Fold Belt.||||||
19462|Warina Sand|44133|5|Briefly described|p158, 152 Fig. 10.2|Middle Eocene|Late Paleocene|Of the Renmark Group. Geological Province: Murray Basin.||||||
19462|Warina Sand|44191|5|Briefly described|Map Legend|Early Eocene|Paleocene|||||||
19462|Warina Sand|49038|4|Described|Table 2|||Briefly described P24.||||||27-OCT-08
19462|Warina Sand|49040|6|Mentioned|p10|||||||||
19462|Warina Sand|50154|5|Briefly described|p132|||Of the Renmark Group. Overlain by the Olney Formation. Geological Province: Murray Basin.||||||
19462|Warina Sand|60451|5|Briefly described|p95 Fig. 61|||||||||
19462|Warina Sand|60452|5|Briefly described|p14, 33|Eocene|Paleocene|Fluvial deposits at the base of the Renmark Group. Formerly referred to as the 'lower' Renmark Beds (Harris, 1966).||||||
19462|Warina Sand|60491|4|Described|p15|Oligocene|Paleocene|Of the Renmark Group. Overlain by the Olney Formation.||||||
19462|Warina Sand|60599|5|Briefly described|p84|Late Paleocene|Late paleocene|Same unit as Warina Formation - names used interchangeably, but probably supersedes Warina Formation? At base of Renmark Group. Fluvial sediments. Geological Province:Murray Basin.||||||07-NOV-08
19462|Warina Sand|61155|5|Briefly described|p2, p18|Early Eocene|Late Paleocene|Of the Renmark Group. Sediments spread in thin sheets over large areas of the Murray Basin. Overlaid by the Olney Formation. Max. thickness: 200m. Age: >62-52Ma. Geological Province: Murray Basin.||||||
19462|Warina Sand|61185|5|Briefly described|p57|Late Paleocene|Middle Paleocene|Base of Renmark Group. Equivalent to White Hills Gravel and Wangerrip Group. Fluvial sediments. Geological Province: Murray Basin. See Warina Formation.||||||07-FEB-11
19462|Warina Sand|61314|6|Mentioned|p129|||Correlates with Renmark beds.||||||
19462|Warina Sand|63887|5|Briefly described|p20, p21 Fig. 1|Early Oligocene|Paleocene|Of Renmark Group. Floodplain and swamp environments dominates, resulting in deposition of carbonaceous sand, clay and silt.||||||
19462|Warina Sand|65552|5|Briefly described|p5 Fig.3, p6|Early Eocene|Late Palaeocene|Of Renmark Group. Fluvial unit of the Murray Basin. Unconformably overlies basement, underlies Olney Formation. c.60 Ma.||||||
19462|Warina Sand|66286|5|Briefly described|p179.|||||Unit in Renmark Group.||Is overlain by Olney Formation.|Poorly consolidated fluvial sands.|
19462|Warina Sand|67462|5|Briefly described|Map legend.|Paleogene|Paleogene|Murray Basin.||Unit in Renmark Group.||||
19462|Warina Sand|68189|5|Briefly described|p25, p26, p27 Tb.3.2|Eocene|Eocene|Braided plain system.||Basal unit of the Renmark Group.||||
19462|Warina Sand|68194|5|Briefly described|p23|||||Unit in Renmark Group.||Is overlain by Olney Formation.|Quartzose sandstone.|
19462|Warina Sand|68715|5|Briefly described|p31 Fig.5|Bartonian|Ypresian|Murray Basin.||Of the Renmark Group.||||
19462|Warina Sand|70718|6|Mentioned|p24|||Oldest sedimentation in the Murray Basin. Fluvial.|~60 Ma|Renmark Group||||30-MAY-19
19462|Warina Sand|71593|5|Briefly described|p52, p54|||||Renmark Group|||Quite pale and clean quartzose pebbly sand.|
19462|Warina Sand|72445|5|Briefly described|App.1, App.7 p5, p7, p8, p16, p20-21.|Paleocene|Paleocene|Characterised by the organic-poor nature of the sands that are a major component of this formation. Said to be non-marine. Suggested (App7 p20) to be equivalent to old 'Lower Renmark Beds'.||Renmark Group||Shown as underlying Olney Formation (sharp contact).|Fine- to coarse grained sand with lignitic fragments , muddy silt with lignite, silty clay and white vein quartz pebbles.|15-OCT-20
19462|Warina Sand|73118|5|Briefly described|p45, 53, 83|Eocene|Paleocene|Glenelg Zone, Western Victoria. Drill core summary log. Entirely concealed. 200m thick. Fluvial deposits.||Renmark Group.||Is overlain by Olney Formation.|Loose to friable grey, brown, poorly to well sorted, medium to coarse sand with minor intercalated fine sand, silt, clay, carbonaceous clay.|
19462|Warina Sand|73228|4|Described|p50-51, p53-57, p60|Early Oligocene|Late Paleocene|Murray Basin. Poorly consolidated fluvial sand. Sandy facies interpreted as a fluvial, braided-channel deposit and the finer grained interbeds as lacustrine and floodplain deposits. Floodplain and swamp sediments also with fluvial and lacustrine depositional environments. Identified in Nadda 1 drillhole. Restricted to deeper parts of the basin.||Renmark Group||Underlain by Coombool Member (Monash Formation). Overlain by Olney Formation.|Pale grey to pale brown medium- to coarse-grained quartz sand with minor thin, lenticular interbeds of locally carbonaceous silt and clay.|
19462|Warina Sand|73229|6|Mentioned|p67|Early Oligocene|Late Paleocene|Murray Basin.||Renmark Group||||
19557|Wataru Gneiss|24197|6|Mentioned|p98|||Only named unit of Birksgate Complex. In the Birksgate Range. Geological Province: Musgrave Block.||||||07-FEB-11
19557|Wataru Gneiss|24496|5|Briefly described|p14|Mesoproterozoic|Mesoproterozoic|Of Birksgate Complex. Massive orthogneiss to gneiss to weakly layered gneiss. Geological Province: Musgrave Block.||||||
19557|Wataru Gneiss|24499|6|Mentioned|Map legend|||||||||
19557|Wataru Gneiss|30923|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
19557|Wataru Gneiss|31965|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
19557|Wataru Gneiss|33478|5|Briefly described|p451|||||||||
19557|Wataru Gneiss|35308|5|Briefly described|p451|||||||||
19557|Wataru Gneiss|40229|5|Briefly described|p28|||||||||
19557|Wataru Gneiss|40910|6|Mentioned|p7|||||||||
19557|Wataru Gneiss|40911|6|Mentioned|Map legend|Mesoproterozoic|Paleoproterozoic|Early-Middle Proterozoic||||||07-NOV-08
19557|Wataru Gneiss|43052|5|Briefly described|p158||Mesoproterozoic|Of Birksgate Complex.||||||14-OCT-08
19557|Wataru Gneiss|43053|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: within Birksgate Complex, Musgrave Block.||||||07-NOV-08
19557|Wataru Gneiss|43258|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
19557|Wataru Gneiss|43298|6|Mentioned|Map Legend||Paleoproterozoic|||||||07-NOV-08
19557|Wataru Gneiss|50607|5|Briefly described|p1.2, 2.7|||Geological Province: Musgrave Block. Of the Birksgate Complex.||||||
19557|Wataru Gneiss|60662|5|Briefly described|Map Legend|||Mixed layered and massive granulites. Of Birksgate Complex.||||||14-OCT-08
19557|Wataru Gneiss|60953|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of the Birksgate Complex. Granulite to amphibolite facies granitic gneiss.||||||
19557|Wataru Gneiss|61108|5|Briefly described|map legend|Mesoproterozoic|Mesoproterozoic|Granitic gneiss, granulite to amphibolite facies.||||||
19557|Wataru Gneiss|65376|6|Mentioned|p9 Fig.1.2. |Mesoproterozoic|Mesoproterozoic||||||Granitic gneiss.|
19557|Wataru Gneiss|67536|6|Mentioned|Map Legend|||Musgrave Block.||Of the Birksgate Complex.|||Massive mainly meta-igneous gneiss and granulite, may include charnockite/migmatite alteration of layered granulite; weakly to moderately magnetic.|02-APR-14
19557|Wataru Gneiss|68131|5|Briefly described|p2 Fig.1|Mesoproterozoic|Mesoproterozoic||||||Granitic gneiss.|
19557|Wataru Gneiss|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||granulite|
19557|Wataru Gneiss|71268|5|Briefly described|1m_geologyp12_lut.csv||||||||Gneiss, granulitic, with hornblende, biotite, orthopyroxene, clinopyroxene|
19557|Wataru Gneiss|73090|5|Briefly described|Appendix.|Mesoproterozoic|Mesoproterozoic||||||Gneiss, granulitic, with hornblende, biotite, orthopyroxene, clinopyroxene.|
19560|Watchie Sandstone|22929|6|Mentioned|27|||Overlying unit Willalinchina Sandstone||||||
19560|Watchie Sandstone|24175|3|Fully described|p35, p32 Fig. 6|Late Miocene|Middle Eocene|Previously of Mirikata Fm. (Ambrose and Flint, 1981b).  Later evidence suggested no correlation so Callen et al (1986) raised its rank. Possibly entirely Oligocene?  Overlies Bulldog Shale.  Max. thickness: <10m.  Geol. Province: Billa Kalina Basin.||||||04-DEC-13
19560|Watchie Sandstone|24321|5|Briefly described|Map legend|Early Pleistocene|Pliocene|||||||
19560|Watchie Sandstone|36966|6|Mentioned|p89|||||||||
19560|Watchie Sandstone|38108|6|Mentioned|Table 1|||||||||
19560|Watchie Sandstone|41257|6|Mentioned|p4|||||||||
19560|Watchie Sandstone|42375|5|Briefly described|p79, p82, p86, p89|||Billa Kalina Basin. Age Miocene? to Pliocene?||||||
19560|Watchie Sandstone|43053|5|Briefly described|Map Legend|Pliocene|Miocene|Lacustrine beach ridges. Geological Province: Billa Kalina Basin.||||||25-MAY-05
19560|Watchie Sandstone|43258|5|Briefly described|Map Legend|Pliocene|Miocene|||||||
19560|Watchie Sandstone|43298|5|Briefly described|Map Legend|Pliocene|Miocene|||||||
19560|Watchie Sandstone|44133|5|Briefly described|p195, 190 Fig. 10.30|Miocene|Miocene|Geological Province: Billa Kalina Basin. Thickness: 7m.||||||
19560|Watchie Sandstone|60953|5|Briefly described|Map Legend|Pliocene|Miocene|Fluviolacustrine sand, often silcreted. Geological Province: Billa Kalina Basin.||||||
19560|Watchie Sandstone|61108|5|Briefly described|map legend|Pliocene|Miocene|Fluviolacustrine sand, often silcreted, and lacustrine beach ridges. Geological Province: Billa Kalina Basin.||||||31-MAY-05
19560|Watchie Sandstone|61155|5|Briefly described|p17|Middle Miocene|Early Miocene|Interfingers with Mirkata Formation. Age: 22.5-13Ma. Geological region: Billa Kalina area.||||||
19560|Watchie Sandstone|66131|6|Mentioned|p242 Fig.2|Miocene|Oligocene|Latest Oligocene to Late Miocene in age (from p.242 Fig.2 - stratigraphic correlation chart).||||||
19560|Watchie Sandstone|67462|5|Briefly described|Map legend.|Miocene|Miocene|Billa Kalina Basin.||||||
19560|Watchie Sandstone|68715|6|Mentioned|p30 Fig.5|Tortonian|Aquitanian|Billa Kalina Basin.||||||
19606|Wattaberri Subgroup|24465|5|Briefly described|p346 Fig.3|||Together with Brown Hill Subgroup, replaced by Bollaparudda Subgroup.||||||24-FEB-05
19606|Wattaberri Subgroup|36836|6|Mentioned|Table 1|||||||||
19606|Wattaberri Subgroup|38873|4|Described|Table 2|||||||||
19607|Wattalunga Sandy Loam|38290|5|Briefly described|p62|||||||||
19626|Waukaringa Siltstone|22510|5|Briefly described|p39, table1|||Of the Upalinna Subgroup.  Age: Marinoan||||||13-OCT-04
19626|Waukaringa Siltstone|22631|6|Mentioned|p178|||Age: Marianoan||||||
19626|Waukaringa Siltstone|32146|6|Mentioned|Fig.3|||||||||
19626|Waukaringa Siltstone|37932|6|Mentioned|p546|||||||||
19626|Waukaringa Siltstone|38110|1|Redefined|p2|Adelaidean|Adelaidean|||||||
19626|Waukaringa Siltstone|41405|3|Fully described|p176|||||||||
19626|Waukaringa Siltstone|41500|4|Described|p80|||||||||
19626|Waukaringa Siltstone|42098|5|Briefly described|p54|||||||||
19626|Waukaringa Siltstone|42109|5|Briefly described|Fif.2 P20|||||||||
19626|Waukaringa Siltstone|42542|5|Briefly described|Fig.2a P11|||||||||
19626|Waukaringa Siltstone|42720|5|Briefly described|map legend|Marinoan||||||||
19626|Waukaringa Siltstone|42813|5|Briefly described|p20|||Of the Farina Subgroup.||||||14-MAY-07
19626|Waukaringa Siltstone|43052|5|Briefly described|p189,Table 6.1|||Of the Farina Subgroup.||||||14-MAY-07
19626|Waukaringa Siltstone|43742|6|Mentioned|Fig.3,p41||Neoproterozoic|||||||
19626|Waukaringa Siltstone|61238|4|Described|p46 Fig. 2, p47 Fig. 3|Neoproterozoic|Neoproterozoic|Of the Umberatana Group. Siltstone and calcareous siltstone.||||||
19626|Waukaringa Siltstone|61732|5|Briefly described|p28 Fig. 13|Marinoan|Marinoan|Of the Upalinna Subgroup (Umberatana Group). Geological Province: Adelaide Rift Complex.||||||07-FEB-11
19626|Waukaringa Siltstone|67030|6|Mentioned|p409 Fig. 2|Cryogenian|Cryogenian|Shown as partial lateral equivalent to Wilmington Formation.||Farina Subgroup||Overlies the Tarcowie Siltstone, underlies the Enorama Shale.||26-APR-12
19626|Waukaringa Siltstone|73093|5|Briefly described|map legend|Neoproterozoic|Neoproterozoic||||||Siltstone, blue-grey, thin bands of limestone and calcareous siltstone.|09-DEC-21
19649|Wearing Dolomite Member|7931|4|Described|p99|Ediacaran|Ediacaran|Described as the basal unit of Wonoka Formation in this study. Max. thickness: 10m.||||||07-FEB-11
19649|Wearing Dolomite Member|22921|5|Briefly described|37|||Of the  Bunyeroo Formation.||||||11-FEB-09
19649|Wearing Dolomite Member|23818|6|Mentioned|p76|||Of the Bunyeroo Formation.||||||
19649|Wearing Dolomite Member|24175|6|Mentioned|p14|Neoproterozoic|Neoproterozoic|||||||
19649|Wearing Dolomite Member|24176|5|Briefly described|p13|Adelaidean|Adelaidean|Of Bunyeroo Formation.  Age is Marinoan.  Geological Province: Mount Painter Province.||||||
19649|Wearing Dolomite Member|24586|5|Briefly described|p51 Fig. 2, p52 Fig. 3|Adelaidean|Adelaidean|Of Haines (1986). Originally the basal part of Wonoka Formation. Upgraded to Wearing Dolomite (Depot Springs Subgroup, Wilpena Group). Geological Province: Adelaide Geosyncline.||||||11-FEB-09
19649|Wearing Dolomite Member|34291|6|Mentioned|p51|||Adelaidean. Bunyeroo Fm||||||
19649|Wearing Dolomite Member|34535|6|Mentioned|p76|||Copper bearing bed||||||
19649|Wearing Dolomite Member|35356|5|Briefly described|p30|||Mineralisation discussed||||||
19649|Wearing Dolomite Member|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Marinoan||||||
19649|Wearing Dolomite Member|41429|3|Fully described|p230|||||||||
19649|Wearing Dolomite Member|41794|6|Mentioned|p790|||||||||
19649|Wearing Dolomite Member|42222|6|Mentioned|p19|||||||||
19649|Wearing Dolomite Member|42238|6|Mentioned|Table 1 P74|||||||||
19649|Wearing Dolomite Member|42600|5|Briefly described|p11|||||||||
19649|Wearing Dolomite Member|43052|6|Mentioned|p194|||of Bunyeroo Formation||||||
19649|Wearing Dolomite Member|43622|6|Mentioned|p38|Neoproterozoic||||||||
19649|Wearing Dolomite Member|60959|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Of the Wonoka Formation. 1-2m thick. Shale and dolomicrite.||||||
19649|Wearing Dolomite Member|61732|5|Briefly described|p28 Fig. 13, p46-47|Marinoan|Marinoan|Basal unit of the Wonoka Formation. Consists of green mudstone with interbeds of brownish calcareous siltstone, pink limestone and maroon and brown mudstone with rare scattered pseudomorphs of gypsum. Geol Prov: Adelaide Rift Complex.||||||07-FEB-11
19649|Wearing Dolomite Member|63397|6|Mentioned|p13|||||||||
19649|Wearing Dolomite Member|64455|5|Briefly described|p137, p138 Fig. 1|Ediacaran|Ediacaran|Of Wonoka Formation. Yellow intraclastic dolomite.||||||29-JAN-09
19649|Wearing Dolomite Member|65892|5|Briefly described|p33-34. |Late Neoproterozoic|Late Neoproterozoic|Abbreviated to Wearing Dolomite on p34.||Unit in Wonoka Formation.|||Lower thin-bedded dolomite under reworked, intraclastic dolomite.|
19649|Wearing Dolomite Member|68030|4|Described|p238-239|Ediacaran|Ediacaran|Flinders Ranges. Represents a hiatus followed by transgressive carbonates over the deepwater siltstones (Bunyeroo Fm).||Unit of Wonoka Formation.||Overlain unconformably by Wonoka Formation. Underlain by Bunyeroo Formation.|Cupriferous, concretionary dolostone, with intraformational and edgewise conglomerates.|
19649|Wearing Dolomite Member|68271|5|Briefly described|p695,697|||Adelaide Rift Complex. Correlative to/overlap in stratigraphic time with Karlaya Limestone (Officer Basin).||Basal unit of Wonoka Formation.||Overlain by Wonoka Formation.||
19649|Wearing Dolomite Member|69019|4|Described|p58-59, p166-167.|||Removed from Bunyeroo Formation by Gostin and Jenkins (1983). 2 to 8 m thick. Hosts veins of barite.||Unit in Wonoka Formation. (Former) unit in Bunyeroo Formation.||Conformably overlies Bunyeroo Formation.|Basal buff to greenish dolomicrite overlain by cyclic 20-30 mm shale interbeds; locally cupriferous; local barite veins.|
19649|Wearing Dolomite Member|70384|5|Briefly described|Map legend.|Ediacaran|Neoproterozoic|Adelaide Geosyncline.||Of Wonoka Formation.|||A thin, cream, laminated dolomite bed; cupriferous.|23-JAN-19
19649|Wearing Dolomite Member|70407|6|Mentioned|p108, 109|||||Superseded name. Of Wonoka Formation.||||
19649|Wearing Dolomite Member|71250|6|Mentioned|p70|Ediacaran|Ediacaran|Central Flinders Ranges.||Wonoka Formation.||Overlies Bunyeroo Formation.||
19649|Wearing Dolomite Member|72456|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Marree 1:250k map sheet.|||||Dolomicrite, green, cupriferous.|
19669|Weedina dolomites|32205|6|Mentioned|p16|||||||||
19685|Weetootla Dolomite|32724|6|Mentioned|Fig.1|||Correlation||||||
19685|Weetootla Dolomite|35255|6|Mentioned|Fig.25|||||||||
19685|Weetootla Dolomite|67180|4|Described|p605-12, Figs. 1, 4, 6, 7|Cryogenian|Cryogenian|Appears numerous times ?as an abbreviation of the Weetootla Dolomite Member, or perhaps intended as an upgrade to Formation rank? Marinoan.||Unit in Upalinna Subgroup||Unconformably overlies the Angepena and Balcanoona Formations, conformably underlies the Amberoona Formation.|Large or giant ooid and stromatolitic limestones; shales; dolomites; lenticular masses of poorly sorted, rounded quartz gravels and sands with lithic fragments infill basal unconformity; clastic conglomerate, calcareous silts.|
19685|Weetootla Dolomite|67979|4|Described|p528, p531 Fig.2, p541|Marinoan||Sturtian-Marinoan Series boundary coincides with erosional basal contact of Weetootla Dolomite (shallow shelf carbonates), and its laterally equivalent, deeper-marine facies, Yankaninna Formation, in Northern Flinders Ranges (Fromhold and Wallace 2011). See also Weetootla Dolomite Member.||Upalinna Subgroup||Unconformably overlies Balcanoona Formation and Angepena Formation; laterally equivalent with Yankaninna Formation (deeper marine facies); overlain conformably/gradationally by Amberoona Formation|Shallow marine carbonates considered transgressive as they overlie subaerial erosion surface|22-SEP-14
19685|Weetootla Dolomite|72613|6|Mentioned|p2 fig 1, p3|Cryogenian|Cryogenian|Shown as earliest  Marinoan age. Northern Flinders Ranges.||Umberatana Group||||
19796|Westbourne Formation|12597|5|Briefly described|p492 Tb.1, p495 Fig.3, p497, p499, p501|Kimmeridgian|Oxfordian|Northern Surat and eastern Eromanga Basins. Thickness generally 80-100m, up to 200m.||Unit in Injune Creek Group.||Conformably overlies Adori Sandstone. Interfingers with Pilliga Sandstone and lower Kumbarilla beds.|Cross-bedded, quartzose to sub-labile sandstone, siltstone and mudstone with lenticular bentonite beds and thin coal seams.|
19796|Westbourne Formation|13497|6|Mentioned|p115 fig 6.33, p130|Late Jurassic|Late Jurassic|Eromanga Basin. See also p141, p144 fig 9.2, p146, p148-p154, p216.||||Overlies the Adori Sandstone. Interfingers with and is overlain by the Namur Sandstone.||
19796|Westbourne Formation|13516|6|Mentioned|p167 fig 10, p169 fig 11, p171 fig 12|Late Jurassic|Late Jurassic|In Eromanga Basin.||||||
19796|Westbourne Formation|22464|6|Mentioned|p9||Late Jurassic|Eromanga Basin. Overlies Adori Sandstone||||||
19796|Westbourne Formation|22857|5|Briefly described|p296-7 Tb.22.1, p314-5|Tithonian|Callovian|Fine-grained sandstone interbedded with siltstone, claystone, minor coal. Max. thickness: 220m. Geological Province: Eromanga Basin. See also p312-3 Fig. 22.6.||||||
19796|Westbourne Formation|22865|4|Described|p314,Table22.1p296-7|Neocomian|Callovian|||||||
19796|Westbourne Formation|22883|6|Mentioned|P31|||||||||
19796|Westbourne Formation|23054|6|Mentioned|Fig5p22|Berriasian|Tithonian|||||||
19796|Westbourne Formation|23056|4|Described|20|||Geol province Eromanga Basin. Of the Injune Creek Group. Underlain by Adori Sandstone.||||||17-JAN-08
19796|Westbourne Formation|23155|5|Briefly described|p26|||The Westbourne Formation has not been recognised on STRZELECKI.||||||
19796|Westbourne Formation|23375|4|Described|Fig2 p265, 291|Tithonian|Tithonian|Laterally equivalent to part of Namur Sandstone. In the Eromanga Basin.||||||17-JAN-08
19796|Westbourne Formation|23425|5|Briefly described|Plate 10.2|||Of Injune Creek Group. Eromanga Basin Province.||||||
19796|Westbourne Formation|23426|5|Briefly described|p403|||Eromanga Basin Province.||||||
19796|Westbourne Formation|23430|4|Described|p523 + p524 Table 14.7|||Of Injune Creek Group. Overlain by Hooray Sandstone - unconformable. Eromanga Basin Province.||||||17-JAN-08
19796|Westbourne Formation|23818|6|Mentioned|p141 Fig.65, p142|Jurassic|Jurassic|Geological Province: Eromanga Basin.||||||
19796|Westbourne Formation|23883|5|Briefly described|p129 Fig. 11.2|Late Jurassic|Late Jurassic|Of the Injune Creek Group.  Geological Province: Great Australian Superbasin.||||||
19796|Westbourne Formation|23982|5|Briefly described|p35 Fig.7|Jurassic|Jurassic|Of Injune Creek Group. Geological Province: Great Artesian Basin.||||||
19796|Westbourne Formation|24068|4|Described|p270 Table 2|Late Jurassic|Late Jurassic|Of Injune Creek Group. Geological Province: Surat Basin.  Maximum thickness: 130m.||||||
19796|Westbourne Formation|24092|5|Briefly described|p8 Fig.3|||Of Injune Creek Group. Geological Province: Eromanga Basin.||||||
19796|Westbourne Formation|24204|5|Briefly described|p266||Jurassic|Geological Province: Eromanga Basin.||||||
19796|Westbourne Formation|24210|5|Briefly described|p133 Fig. 2|Late Jurassic|Late Jurassic|Geological Province: Eromanga Basin.||||||
19796|Westbourne Formation|29591|6|Mentioned|Table 15|||||||||
19796|Westbourne Formation|30021|6|Mentioned|p90|||||||||
19796|Westbourne Formation|30024|6|Mentioned|p332|||||||||
19796|Westbourne Formation|30102|5|Briefly described|p24|||Unit of the Injune Creek Group. See also P21,25,31,34.||||||
19796|Westbourne Formation|30103|5|Briefly described|p9|||Table 3 on P9. Upper Jurassic age.||||||
19796|Westbourne Formation|30104|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle to Upper Jurassic.M - U||||||
19796|Westbourne Formation|30508|6|Mentioned|p92|||Stratigraphic drilling||||||
19796|Westbourne Formation|30691|4|Described|p15|||See also Table 4. Upper Jurassic age||||||
19796|Westbourne Formation|30692|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|||||||
19796|Westbourne Formation|30695|4|Described|Table 4|||Middle-Upper Jurassic||||||
19796|Westbourne Formation|30696|4|Described|Table 4|||Middle-Upper Jurassic||||||
19796|Westbourne Formation|30699|6|Mentioned|p56|||Map||||||
19796|Westbourne Formation|30700|6|Mentioned|p27|||||||||
19796|Westbourne Formation|30702|6|Mentioned|Fig.1|||See also Table 1. Stratigraphic table||||||
19796|Westbourne Formation|30804|6|Mentioned|Table 2|||||||||
19796|Westbourne Formation|30853|5|Briefly described|Table 3|||Upper Jurassic age||||||
19796|Westbourne Formation|30854|4|Described|Table 4|||Upper Jurassic age||||||
19796|Westbourne Formation|30855|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|Unit in Injune Creek Group||||||
19796|Westbourne Formation|30856|4|Described|Table 3|||On p10. Upper Jurassic age.||||||17-JAN-08
19796|Westbourne Formation|30857|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|Part of Injune Creek Group||||||
19796|Westbourne Formation|31116|4|Described|p36|||See also p27.||||||17-JAN-08
19796|Westbourne Formation|31120|6|Mentioned|Table 1|||||||||
19796|Westbourne Formation|31145|5|Briefly described|Table 1|||U. Jurassic||||||
19796|Westbourne Formation|31425|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|||||||
19796|Westbourne Formation|31431|5|Briefly described|Table 3|||M.-U.Jurassic||||||
19796|Westbourne Formation|31553|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle to Upper JurassicM - U||||||
19796|Westbourne Formation|32138|6|Mentioned|p396|||||||||
19796|Westbourne Formation|32193|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle to Upper JurassicM - U||||||
19796|Westbourne Formation|33067|4|Described|Table 1|Late Jurassic|Jurassic|Of the Injune Creek Group.  Siltstone, shale, quartz sandstone.||||||07-JUL-04
19796|Westbourne Formation|33069|4|Described|p7|||U.Jur.||||||
19796|Westbourne Formation|33071|5|Briefly described|p6|||M.-U.Jur.||||||
19796|Westbourne Formation|33075|6|Mentioned|p445|||||||||
19796|Westbourne Formation|33078|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|||||||
19796|Westbourne Formation|33079|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|||||||
19796|Westbourne Formation|33080|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle to Upper JurassicM - U||||||
19796|Westbourne Formation|33082|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|||||||
19796|Westbourne Formation|33086|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle to Upper JurassicM - U||||||
19796|Westbourne Formation|33087|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|||||||
19796|Westbourne Formation|33088|4|Described|Table 3|||U.Jur.||||||
19796|Westbourne Formation|33089|5|Briefly described|Table 2|||M.-U.Jur.||||||
19796|Westbourne Formation|33092|5|Briefly described|p9|||Stratigraphy||||||
19796|Westbourne Formation|33176|6|Mentioned|p175|||Correlated with Loth Fm.||||||
19796|Westbourne Formation|33183|6|Mentioned|p233|||||||||
19796|Westbourne Formation|33367|3|Fully described|p26|||||||||
19796|Westbourne Formation|33371|2|Defined|p58|Jurassic|Jurassic|See also p59. Prob. Jurassic.||||||17-JAN-08
19796|Westbourne Formation|33449|4|Described|Table 1|||U.Jur.||||||
19796|Westbourne Formation|33638|5|Briefly described|Table 1|||||||||
19796|Westbourne Formation|33639|5|Briefly described|Table 2|||||||||
19796|Westbourne Formation|33640|4|Described|Table 3|||M.-U.Jur.||||||
19796|Westbourne Formation|33643|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|||||||
19796|Westbourne Formation|33648|6|Mentioned|p19|||Stratigraphy.||||||
19796|Westbourne Formation|33672|5|Briefly described|p44|||Lithology.||||||
19796|Westbourne Formation|33673|4|Described|p291|||See also p287||||||17-JAN-08
19796|Westbourne Formation|33821|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|||||||
19796|Westbourne Formation|33825|5|Briefly described|p9,10|||Equiv. correl. Lithology. Correlation table.||||||
19796|Westbourne Formation|33827|6|Mentioned|p13|||||||||
19796|Westbourne Formation|33939|6|Mentioned|p412|||||||||
19796|Westbourne Formation|33998|6|Mentioned|p31|||||||||
19796|Westbourne Formation|34065|4|Described|p7|||U.Jur.||||||
19796|Westbourne Formation|34091|5|Briefly described|Table 1|||Jur.||||||
19796|Westbourne Formation|34134|6|Mentioned|Cor.Chart|||Middle Jurassic||||||
19796|Westbourne Formation|34174|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle - Upper JurassicM - U||||||
19796|Westbourne Formation|34218|4|Described|Table 1|||Upper Jurassic. See also Table 2.||||||
19796|Westbourne Formation|34386|6|Mentioned|p97|||Jurassic. See also P98,99,100 etc.||||||
19796|Westbourne Formation|34486|4|Described|Table 1|||See also Table 2, p10. Upper Jurassic.||||||17-JAN-08
19796|Westbourne Formation|34487|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle - Upper JurassicM - U||||||
19796|Westbourne Formation|34611|6|Mentioned|Fig.65|||Correlation chart.||||||
19796|Westbourne Formation|35239|6|Mentioned|Table 1|||||||||
19796|Westbourne Formation|35560|6|Mentioned|p289|||||||||
19796|Westbourne Formation|35562|6|Mentioned|Table 4|||Biostratigraphy||||||
19796|Westbourne Formation|35663|5|Briefly described|p126|||||||||
19796|Westbourne Formation|35811|5|Briefly described|Table 3|||||||||
19796|Westbourne Formation|35937|6|Mentioned|Fig.5|||||||||
19796|Westbourne Formation|36243|6|Mentioned|Table 6A|||||||||
19796|Westbourne Formation|36251|6|Mentioned|Fig.2|||||||||
19796|Westbourne Formation|36570|6|Mentioned|p55|||||||||
19796|Westbourne Formation|36910|6|Mentioned|Fig.3|||||||||
19796|Westbourne Formation|37117|5|Briefly described|p313|||||||||
19796|Westbourne Formation|37287|6|Mentioned|p36|||||||||
19796|Westbourne Formation|37608|3|Fully described|Table 1|||||||||
19796|Westbourne Formation|37995|4|Described|p64|||||||||
19796|Westbourne Formation|38199|6|Mentioned|p423|||||||||
19796|Westbourne Formation|38226|6|Mentioned|Table 1|||||||||
19796|Westbourne Formation|38779|6|Mentioned|p7|||||||||
19796|Westbourne Formation|39070|4|Described|p363|||||||||
19796|Westbourne Formation|39212|5|Briefly described|p16|||See also P38||||||
19796|Westbourne Formation|39276|6|Mentioned|Fig. 2|||||||||
19796|Westbourne Formation|39445|5|Briefly described|Table 10|||||||||
19796|Westbourne Formation|39478|6|Mentioned|Table 1|||||||||
19796|Westbourne Formation|39494|6|Mentioned|p129|||See also Figs 3,5||||||
19796|Westbourne Formation|39846|6|Mentioned|p45|||||||||
19796|Westbourne Formation|39847|5|Briefly described|p36|||||||||
19796|Westbourne Formation|39914|6|Mentioned|p2|||||||||
19796|Westbourne Formation|39943|6|Mentioned|Table 8A|||||||||
19796|Westbourne Formation|39988|6|Mentioned|p289|||||||||
19796|Westbourne Formation|39989|4|Described|p422|||||||||
19796|Westbourne Formation|40030|6|Mentioned|Fig.3|||||||||
19796|Westbourne Formation|40121|6|Mentioned|p446|||||||||
19796|Westbourne Formation|40199|6|Mentioned|Fig.1|||||||||
19796|Westbourne Formation|40245|6|Mentioned|Table 2|||||||||
19796|Westbourne Formation|40249|6|Mentioned|p38|||Mention P41||||||
19796|Westbourne Formation|40250|6|Mentioned|Fig.7|||||||||
19796|Westbourne Formation|40540|6|Mentioned|p155|||||||||
19796|Westbourne Formation|40541|3|Fully described|p110|||||||||
19796|Westbourne Formation|40544|6|Mentioned|p159|||See also Fig.6||||||
19796|Westbourne Formation|40666|4|Described|p357|||||||||
19796|Westbourne Formation|40670|6|Mentioned|Fig.9|||||||||
19796|Westbourne Formation|40675|6|Mentioned|Table 8A|||Mention Table 9A||||||
19796|Westbourne Formation|40687|3|Fully described|p416|||||||||
19796|Westbourne Formation|40832|3|Fully described|p456|||||||||
19796|Westbourne Formation|40833|6|Mentioned|p468|||||||||
19796|Westbourne Formation|40910|6|Mentioned|Table 3|||||||||
19796|Westbourne Formation|40926|6|Mentioned|Table 2|||||||||
19796|Westbourne Formation|40962|6|Mentioned|Table 1|||||||||
19796|Westbourne Formation|41060|6|Mentioned|p7|||Generalized stratigraphy||||||
19796|Westbourne Formation|41061|6|Mentioned|p19|||||||||
19796|Westbourne Formation|41062|6|Mentioned|p27|||See also P34 and Fig.5||||||
19796|Westbourne Formation|41063|6|Mentioned|p40|||||||||
19796|Westbourne Formation|41064|6|Mentioned|p60|||||||||
19796|Westbourne Formation|41084|5|Briefly described|p80|||See also Fig.2||||||
19796|Westbourne Formation|41097|6|Mentioned|Table 1|||||||||
19796|Westbourne Formation|41099|6|Mentioned|p192|||||||||
19796|Westbourne Formation|41123|6|Mentioned|p177|||||||||
19796|Westbourne Formation|41175|5|Briefly described|p195|||||||||
19796|Westbourne Formation|41176|6|Mentioned|Table 2|||||||||
19796|Westbourne Formation|41177|6|Mentioned|p222|||||||||
19796|Westbourne Formation|41182|5|Briefly described|Fig.2|||||||||
19796|Westbourne Formation|41183|6|Mentioned|p310|||||||||
19796|Westbourne Formation|41186|4|Described|p208|||||||||
19796|Westbourne Formation|41187|6|Mentioned|Fig.2|||||||||
19796|Westbourne Formation|41198|6|Mentioned|Table 1|||||||||
19796|Westbourne Formation|41210|5|Briefly described|Fig.3|||||||||
19796|Westbourne Formation|41214|6|Mentioned|Fig.3|||||||||
19796|Westbourne Formation|41216|6|Mentioned|p300|||See also Fig.18||||||
19796|Westbourne Formation|41219|4|Described|p346|||||||||
19796|Westbourne Formation|41247|6|Mentioned|p120|||||||||
19796|Westbourne Formation|41266|6|Mentioned|Fig.3|||||||||
19796|Westbourne Formation|41681|6|Mentioned|p10|||See also P13||||||
19796|Westbourne Formation|41707|5|Briefly described|p163|||||||||
19796|Westbourne Formation|41724|6|Mentioned|p382|||||||||
19796|Westbourne Formation|41992|4|Described|Fig.2 P183|||||||||
19796|Westbourne Formation|42007|5|Briefly described|Fig.2 P182|||||||||
19796|Westbourne Formation|42061|4|Described|Fig,11 P159|||||||||
19796|Westbourne Formation|42067|4|Described|p308|||See also appendix 2||||||
19796|Westbourne Formation|42071|6|Mentioned|p117|||||||||
19796|Westbourne Formation|42084|6|Mentioned|Fig.3 P356|||||||||
19796|Westbourne Formation|42085|6|Mentioned|Fig.2 P374|||||||||
19796|Westbourne Formation|42397|5|Briefly described|p10|||||||||
19796|Westbourne Formation|42446|4|Described|p12|||||||||
19796|Westbourne Formation|42447|5|Briefly described|p5 + Fig. 1|||||||||
19796|Westbourne Formation|42463|6|Mentioned|Fig.5 P172|||||||||
19796|Westbourne Formation|42474|6|Mentioned|p25|||||||||
19796|Westbourne Formation|42493|5|Briefly described|p20, Fig.1 p18|||||||||
19796|Westbourne Formation|42496|5|Briefly described|p136, Fig.3 p132|||||||||
19796|Westbourne Formation|42520|5|Briefly described|p6|||||||||
19796|Westbourne Formation|42634|6|Mentioned|p12|||||||||
19796|Westbourne Formation|42746|5|Briefly described|p9, p10|||See also Fig.6 P8, Fig.7 P37||||||
19796|Westbourne Formation|42749|4|Described|p30, Fig.5 p29|||see also Fig.2 p27.||||||17-JAN-08
19796|Westbourne Formation|42999|5|Briefly described|Table 2,p90||Late Jurassic|||||||
19796|Westbourne Formation|43000|5|Briefly described|Fig.5,p112|||of Injune Creek Group||||||
19796|Westbourne Formation|43002|5|Briefly described|Fig.2,p135|||||||||
19796|Westbourne Formation|43004|5|Briefly described|Table 1,p179|||||||||
19796|Westbourne Formation|43105|5|Briefly described|Fig.9,p15.|||||||||
19796|Westbourne Formation|43114|5|Briefly described|p12|||||||||
19796|Westbourne Formation|43122|5|Briefly described|p11|||see also Fig. 2.||||||
19796|Westbourne Formation|43404|14|Not recorded|Table p11||Late Jurassic|||||||
19796|Westbourne Formation|43591|6|Mentioned|p40|||||||||
19796|Westbourne Formation|43628|6|Mentioned|Fig.13||Late Jurassic|||||||
19796|Westbourne Formation|43711|6|Mentioned|p18|||||||||
19796|Westbourne Formation|43989|14|Not recorded|Map Legend|Late Jurassic|Middle Jurassic|||||||
19796|Westbourne Formation|44016|14|Not recorded|Map Legend||Late Jurassic|||||||
19796|Westbourne Formation|44019|14|Not recorded|Map Legend||Late Jurassic|||||||
19796|Westbourne Formation|44020|14|Not recorded|Tb.1,2|Late Jurassic|Middle Jurassic|Of Injune Creek Group.||||||
19796|Westbourne Formation|44021|14|Not recorded|p232-234,236-238||Late Jurassic|="Upper Intermediate Series" of Woolley 1941. Is upper part of Injune Creek Group. Overlies Birkhead Formation. Overlain by "Hooray Sandstone". Overlies Adori Sandstone. Plants and spores.||||||
19796|Westbourne Formation|44022|14|Not recorded|Map Legend||Late Jurassic|||||||
19796|Westbourne Formation|44023|4|Described|Tb.3,p12||Late Jurassic|||||||
19796|Westbourne Formation|44027|14|Not recorded|p110||Late Jurassic|||||||
19796|Westbourne Formation|44028|14|Not recorded|Fig.2,7,p514||Jurassic|Of Injune Creek Group. See Strat Table.||||||
19796|Westbourne Formation|44031|14|Not recorded|p5,8,12,13||Jurassic|||||||
19796|Westbourne Formation|44084|14|Not recorded|p32(Tb)|||||||||
19796|Westbourne Formation|44133|5|Briefly described|p110, 104 Fig. 9.11|Early Cretaceous|Late Jurassic|Geological Province: Eromanga Basin. Conformably overlies: Adori Sandstone. Overlain and intertongued by Namur Sandstone.||||||28-SEP-16
19796|Westbourne Formation|44171|14|Not recorded|p194,19,197,198|||||||||
19796|Westbourne Formation|44337|5|Briefly described|Map Legend||Jurassic|Lithology.||||||
19796|Westbourne Formation|44374|14|Not recorded|p11|Cretaceous|Jurassic|||||||
19796|Westbourne Formation|44414|14|Not recorded|p112-115|Cretaceous|Jurassic|||||||
19796|Westbourne Formation|44415|14|Not recorded|Fig.2,p23|||||||||
19796|Westbourne Formation|45071|3|Fully described|Table 15|||See also p82.||||||17-JAN-08
19796|Westbourne Formation|45110|2|Defined|p97|Late Jurassic|Late Jurassic|See also Fig.5 and p24.||||||17-JAN-08
19796|Westbourne Formation|46791|6|Mentioned|Table 1|||||||||
19796|Westbourne Formation|46937|5|Briefly described|Fig.10|||See also Table 1.||||||
19796|Westbourne Formation|46939|6|Mentioned|Fig.2|||See also Fig.1.||||||
19796|Westbourne Formation|46984|6|Mentioned|Table 1|||||||||
19796|Westbourne Formation|48919|4|Described|p63|||U.Jurassic. See also p64-65.||||||17-JAN-08
19796|Westbourne Formation|48920|3|Fully described|p53|||Part of Injune Creek Group.||||||16-SEP-08
19796|Westbourne Formation|49010|6|Mentioned|Fig.4|||Eromanga Basin||||||
19796|Westbourne Formation|49011|6|Mentioned|Fig.3|||Eromanga Basin||||||
19796|Westbourne Formation|60717|5|Briefly described|p40 Fig. 2|Late Jurassic|Late Jurassic|Overlies Adori Sandstone; overlain by Murta Formation; lateral to Adori Sandstone? Geological Province: Eromanga  Basin.||||||31-JAN-08
19796|Westbourne Formation|60993|5|Briefly described|p36|||Of the Injune Creek Group. May be the equivalent of the upper sandstone section of the Woodenbong beds. Geological Province: Surat Basin.||||||
19796|Westbourne Formation|60999|5|Briefly described|p178 Fig. 10|||Geological Province: Surat Basin.||||||
19796|Westbourne Formation|61000|5|Briefly described|p186 Fig. 4|Tithonian|Callovian|Geological Province: Surat Basin.||||||
19796|Westbourne Formation|61312|5|Briefly described|p67 Fig. E5|Late Jurassic|Jurassic|Of the Injune Creek Group. Siltstone, shale and fine-grained quartzose sandstone; productive reservoir unit. Geological Province: Eromanga Basin. See also p79 Table E2.||||||
19796|Westbourne Formation|61377|5|Briefly described|p148 Tb. SU1|Late Jurassic|Jurassic|Shale, siltstone, quartz sandstone, minor coal. Geological Province: Surat Basin. See also p149 Fig. SU8.||||||07-FEB-11
19796|Westbourne Formation|61611|6|Mentioned|p265 Fig. 3|Late Jurassic|Early Cretaceous|Geological Province: Surat Basin and Eromanga Basin.||||||13-MAR-09
19796|Westbourne Formation|61613|6|Mentioned|p282 Fig. 2|Early Cretaceous|Late Jurassic|Geological Province: Eromanga Basin.||||||07-FEB-11
19796|Westbourne Formation|61614|6|Mentioned|p290 Fig. 2|Late Jurassic|Late Jurassic|Geological Province: Eromanga Basin.||||||17-MAR-09
19796|Westbourne Formation|61615|6|Mentioned|p302 Fig. 2|Late Jurassic|Late Jurassic|Geological Province: Eromanga Basin.||||||07-FEB-11
19796|Westbourne Formation|61823|5|Briefly described|p118|Cretaceous|Jurassic|Fluvial-lacustrine sediments. Geological Province:  Eromanga Basin.||||||
19796|Westbourne Formation|62730|5|Briefly described|p352 Fig. 1|Late Jurassic|Late Jurassic|Geological Province: Eromanga Basin.||||||21-APR-08
19796|Westbourne Formation|63218|6|Mentioned|p211 Fig.2. |Late Jurassic|Late Jurassic|Surat Basin.||Unit in Injune Creek Group.|Includes Norwood Mudstone Member.|Overlies Springbok Sandstone.||
19796|Westbourne Formation|63979|4|Described|p38-39, Fig. 44|Tithonian|Oxford|Conformable on Adori Sst; overlain by/intertongues with Hooray Sst. and "upper Namur Sst". Max.thickness:166m. Fine to v.fine, rarely med.- to coarse-gr. sst, moderately to poorly sorted, interlaminated/interbedded with siltst.+ shale. In Eromanga Basin.||||||07-FEB-11
19796|Westbourne Formation|64048|5|Briefly described|p64 Tb. 2, p70|||Geological Province: Eromanga Basin. Possesses some hydrocarbon source potential.||||||07-FEB-11
19796|Westbourne Formation|64197|6|Mentioned|p625 Fig.1c, p630 Fig.7|Late Jurassic|Late Jurassic|Eromanga and Surat/Bowen Basins.||||Eromanga Basin: overlies Adori Sandstone; underlies Hooray Sandstone. Surat/Bowen Basins: overlies Springbok Sandstone; underlies Gubberamunda Sandstone.||11-DEC-15
19796|Westbourne Formation|64665|5|Briefly described|p53 Fig.2, p60.|Late Jurassic|Late Jurassic|Eromanga and Surat Basins. Contains thin coals.||Upper unit in Injune Creek Group.||Overlies Adori and Springbok Sandstones.||
19796|Westbourne Formation|64856|3|Fully described|p79, p88-95|Tithonian|Oxfordian|Defined by American Overseas Petroleum Ltd (1964) with a type section 389-503m in AOP Westbourne 1 well. Eromanga and Surat Basins. Interbedded shales and siltstones and very fine-grained, quartzose sandstones. Includes Norwood Mudstone Member. Conformably overlies the Springbok Sandstone, intertongues and grades into the Pilliga Sandstone to south. Underlies Gubberamunda Sandstone. Up to 220m thick. Age from palynoflora (units APJ5, 6).||||||18-JAN-22
19796|Westbourne Formation|64857|5|Briefly described|p113 Fig.3, p115|||Overlies Springbok Sandstone, Surat Basin.||||||
19796|Westbourne Formation|64858|6|Mentioned|p181 Tb.1, p187-188|||Surat Basin.||||||30-NOV-09
19796|Westbourne Formation|65003|5|Briefly described|p8||Jurassic|Of Surat Basin.||||||
19796|Westbourne Formation|65112|5|Briefly described|p323; p328; Fig 11 p 324; fig 16 p328|Jurassic|Jurassic||156-142 Ma.|||Overlies Springbok Sandstone, underlies Gubberamunda Sandstone.|Non-marine, upward-fining clastic sedimentary rock. A package with a lower sand-rich part, followed by a shale-rich unit.|22-MAR-12
19796|Westbourne Formation|65113|5|Briefly described|Fig 4 p340|Late Jurassic|Late Jurassic|Overlies the Springbok Formation, underlies Gubberamunda Sandstone.||||||
19796|Westbourne Formation|65114|5|Briefly described|p385 Fig.3|Late Jurassic||||||||
19796|Westbourne Formation|65116|5|Briefly described|Fig 2 p437|Late Jurassic|Late Jurassic|Underlies the Gubberamunda Sandstone, overlies the Springbok Sandstone, Surat Basin.||||||06-MAR-12
19796|Westbourne Formation|65117|5|Briefly described|p463, 471-472,  474,  Fig 4 p465|Tithonian|Oxfordian|Surat Basin, up to 200m thick. Conformable on Springbok Sandstone. Diachronous base. Older in Surat than Eromanga Basins. Interbedded mudstone, siltstone, coal and very fine grained quartzose to lithic-feldspathic sandstone.||||||
19796|Westbourne Formation|65119|6|Mentioned|Fig 6 p512, Fig 13-14|||Present in the Cabawin 1 and Rockwood 1 wells.||||||07-MAR-12
19796|Westbourne Formation|65238|5|Briefly described|p10|||Geological province: Eromanga Basin. Overbank and lacustrine-swamp deposits.||||||
19796|Westbourne Formation|65385|5|Briefly described|pS134 Fig.7|Late Jurassic|Late Jurassic|Of Eromanga Basin. Overlies Adori Sandstone. Sediment with volcanic component. See also "uppermost Westbourne Formation".||||||08-MAR-12
19796|Westbourne Formation|65489|5|Briefly described|p15, p49, p96, p155|Late Jurassic|Late Jurassic|Eromanga Basin. 210m thick. Fair source rock. Potential for stratigraphic structural traps. Oil reservoir accounting for 4% of the Basin's production.||||Overlies Adori Sandstone. Is overlain by Namur Sandstone.||
19796|Westbourne Formation|66529|6|Mentioned|p12 Fig.5|||Eromanga Basin.||Unit in Injune Creek Group.||Overlies Adori or Springbok Sandstones. Is overlain by Namur, Hooray or Gubberamunda Sandstones.||
19796|Westbourne Formation|66623|6|Mentioned|p239.|Early Cretaceous|Late Jurassic|||||||
19796|Westbourne Formation|66915|5|Briefly described|p6 Fig.3|Early Cretaceous|Late Jurassic|Eromanga and Surat Basins. In Fig.3 also shows "uppermost Westbourne Formation" in Eromanga Basin.||Injune Creek Group||||
19796|Westbourne Formation|67133|5|Briefly described|p2, p5, p15-16, p18-21|Jurassic|Jurassic|32 samples of this unit were analysed by XRD and optical microscopy for this study. Deposited in a lacustrine delta environment. Quartz is the main component (18-80%) with feldspars (12-40%); plagioclase is always dominant. Kaolinite (up to 33%) is the dominant clay mineral. The mixed-layer clays are highly variable.||||Conformably overlies Springbok Sandstone. Is overlain by Gubberamunda Sandstone.|Very fine- to medium-grained, fairly to poorly sorted, sublabile to quartzose, often massive sandstones with laminated to thinly-bedded siltstones and shales.|
19796|Westbourne Formation|67323|5|Briefly described|p87-88, p93, p95 Fig.12.5|Late Jurassic|Late Jurassic|Eromanga Basin. Hydrocarbon exploration target in the Basin.||||Overlies Adori Sandstone. Is overlain by Hooray Sandstone.||
19796|Westbourne Formation|67402|4|Described|p26, p26 tbl RRM4, p108|Berriasian|Oxfordian|Eromanga Basin. Potential conventional seal for the storage of carbon dioxide. Proven seal of the Springbok Formation. Deposited in fluvial to fluvio-lacustrine environments during a series of regressive-transgressive cycles. Maximum thickness of 160m. Demonstrated hydrocarbon seal. See also p109, p113, p115, p123, p146, p148, p151, p152, p154 fig SRT15/16, p156, p226, p265.||||Overlies the Adori Sandstone. Conformably overlies the Springbok Sandstone. Overlain by the Hooray Sandstone.|Fine to very fine-grained sandstone, interlaminated and interbedded with siltstone and shale.|
19796|Westbourne Formation|67561|5|Briefly described|p52 Fig.2, p58 Fig.7, p59 Fig.8|Valanginian|Berriasian|Australian Spore-Pollen zonation: C.watherooensis.||||||
19796|Westbourne Formation|68003|5|Briefly described|p57 Fig.3-n.|||Bowen Basin.||Unit in Injune Creek Group.||Overlies Springbok Sandstone. Is overlain by Gubberamunda Sandstone.||
19796|Westbourne Formation|68117|5|Briefly described|p345-346|Late Jurassic|Late Jurassic|Surat Basin.||Injune Creek Group.|Norwood Mudstone Member.|Overlies Springbok Sandstone.||
19796|Westbourne Formation|68135|5|Briefly described|p52 fig 2b, p57 fig 4|Tithonian|Kimmeridgian|Surat Basin (QLD) and Eromanga Basin.||||Overlies Springbok and Adori Sandstones. Is unconformably overlain by Gubberamunda, Hooray and Namur Sandstones.|Interbedded sandstone and siltstone.|15-SEP-17
19796|Westbourne Formation|68139|6|Mentioned|p23|Late Jurassic|Late Jurassic|Surat Basin.||Injune Creek Group.||Unconformably overlies Springbok Sandstone. Is overlain by Gubberamunda Sandstone.||
19796|Westbourne Formation|68279|6|Mentioned|p18-19|||Galilee Basin stratigraphic cross-sections, and mineralogy tables.||||||
19796|Westbourne Formation|68576|5|Briefly described|Q_4: p3|Late Jurassic|Late Jurassic|Surat Basin.||Injune Creek Group.||Overlies Springbok Sandstone. Is overlain unconformably by Gubberamunda Sandstone.||
19796|Westbourne Formation|68731|6|Mentioned|pp209-211|||||||||
19796|Westbourne Formation|69001|6|Mentioned|p16|Early Cretaceous|Jurassic|Recent interpretations by the NSW DPI broadly group this unit within the Algebuckina Sandstone and equivalent units.||||||
19796|Westbourne Formation|69019|5|Briefly described|p85 Fig.21.|Berriasian|Tithonian|Southern Eromanga Basin.||||Overlies Adori Sandstone. Is overlain by Namur Sandstone.||
19796|Westbourne Formation|69023|6|Mentioned|p89 Fig.20, p91|Berriasian|Tithonian|||||Intertongues with lower part of Namur Sandstone.||
19796|Westbourne Formation|69457|6|Mentioned|p41:3-4|||Eromanga Basin.||||||12-JUL-16
19796|Westbourne Formation|69582|5|Briefly described|p36, p38, p65-p66|Late Jurassic|Late Jurassic|Eromanga Basin. Intersected in GSQ Longreach 2 drillhole.||||Overlies the Springbok Sandstone and the Adori Sandstone. Unconformably overlain by the Gubberamunda Sandstone. Overlain by the Hooray Sandstone.|Mudstone, sandstone, siltstone.|
19796|Westbourne Formation|69594|3|Fully described|p519, p525-527, p531, p537, p573|Tithonian|Kimmeridgian|Exon (1966). Swarbrick et al. (1973) defined the lower part as the Norwood Mudstone Member. Eromanga, northern Surat Basins. The type section is 390-503m in AOP Westbourne 1, near Tambo. Discrimination from Adori Sandstone described. Along the SA border, the Namur Sandstone, Westbourne Formation and Adori Sandstone cannot be delineated. Up to 250m thick. Basal fluviatile, later lacustrine deposits. Has hydrocarbon source potential; is a significant reservoir. RELATED UNITS (continued): Is overlain by and interfingers with both Namur and Hooray Sandstones; is overlain conformably to unconformably by the upper Namur Sandstone; and Gubberamunda Sandstone conformably (locally disconformably).||Injune Creek Group.|Norwood Mudstone Member.|Conformably overlies Adori and Springbok Sandstones. Interdigitates with and passes into Pilliga Sandstone. See COMMENTS for more.|Fine, very fine, rarely medium or coarse, labile micaceous sandstones with interbedded siltstone and shale.|
19796|Westbourne Formation|69673|6|Mentioned|p154, p155 fig 127|Cretaceous|Jurassic|||||Overlies Adori Sandstone, overlain by Namur Sandstone||
19796|Westbourne Formation|69681|6|Mentioned|p74 Fig.3, p82|Late Jurassic|Late Jurassic|Mineralogy and likely chemical changes from CO2 injection discussed.||Unit in Injune Creek Group.||||
19796|Westbourne Formation|69682|5|Briefly described|p95 Fig.3|Late Jurassic|Late Jurassic|Surat Basin.||Unit in Injune Creek Group.||Overlies Springbok Sandstone. Is overlain by Gubberamunda Sandstone.||
19796|Westbourne Formation|69790|6|Mentioned|p1063 Fig.2, p1068 Fig.7|Late Jurassic|Late Jurassic|Eromanga Basin.||Unit in Injune Creek Group.||||
19796|Westbourne Formation|69797|5|Briefly described|p17 Fig.2|Late Jurassic|Late Jurassic|Geol. Prov: Eromanga Basin. Presented in figure as Westbourne Fm.||||||
19796|Westbourne Formation|69946|3|Fully described|p11, p15-16, p24, p57-58|Early Cretaceous|Late Jurassic|Named by Gerrard (1964) in an unpublished well completion report; Exon (1966) published the definition and assigned the type section: the interval 389.8 - 503.0m in Westbourne 1. Restricted to N Cooper region and easternmost Pedirka region in SA. 30 - 140m thick. Eromanga Basin. Wireline log correlations.||||Conformably overlies Adori Sandstone. Intertongues with overlying Namur and Algebuckina Sandstones.|Interbedded dark grey shale and siltstone with minor sandstone interbeds.|
19796|Westbourne Formation|69947|5|Briefly described|p7-8, p13 Fig.7.2, p31 Fig.7.20|Early Cretaceous|Late Jurassic|Eromanga Basin. Forms a couplet with Adori Sandstone, restricted to northern Cooper region and eastern-most Perdika region.||||Gradationally overlies Adori Sandstone. Is overlain by Namur Sandstone.|Dark grey shale, siltstone and minor sandstone interbeds.|
19796|Westbourne Formation|70374|6|Mentioned|p809 figure 1, p814|Tithonian|Kimmeridgian|Surat Basin.||Injune Creek Group||Overlies ?conformably Springbok Sandstone.||28-SEP-16
19796|Westbourne Formation|70628|6|Mentioned|p952, Fig 4|Kimmeridgian|Kimmeridgian|Shown only as 'Westbourne' in fig 4. Along with Gubberamunda [Sandstone], Springbok Formation,  forms part of the L-sequence (Hoffman et al 2009) of the Surat Basin.||||Underlies Gubberamunda Sandstone. Overlies Springbok Formation.||
19796|Westbourne Formation|70821|5|Briefly described|p21 Fig.2.6, p80|Jurassic|Jurassic|Eromanga and Surat Basins. Aquitard.||Injune Creek Group.||Overlies Adori Sandstone and Springbok Sandstone. Is overlain by Namur Sandstone, Hooray Sandstone and Gubberamunda Sandstone.||
19796|Westbourne Formation|70823|5|Briefly described|p25-p27, p43, p78|Late Jurassic|Middle Jurassic|Eromanga Basin. Deposited in low-energy meandering fluvial and overbank floodplain environments.||||Overlies the Adori Sandstone. Overlain by the Namur Sandstone.||
19796|Westbourne Formation|70824|5|Briefly described|p9|Jurassic|Jurassic|Eromanga Basin.||||Overlies the Adori Sandstone. Overlain by the Murta Formation and the Hooray and Namur Sandstones.||
19796|Westbourne Formation|70860|6|Mentioned|p281|||Great Artesian Basin.||||||
19796|Westbourne Formation|71282|6|Mentioned|p457 Fig.1|||Appears just as Westbourne in Fig.1.||||||
19796|Westbourne Formation|71321|6|Mentioned|p15|||Of Eromanga Basin.||||||
19796|Westbourne Formation|71342|4|Described|Ch1 p19, Ch5 p12, Ch5 p15-p17, Ch5 p24|Berriasian|Tithonian|Originally defined by Gerrard (1964) in the Boree 1 unpublished well completion report, however, it was first published by Exon (1966) who defined it and assigned the type section. The type section is in Westbourne 1 in Queensland (Exon, 1966). This unit is generally 30 to 140m thick in the Cooper region. Spore-pollen zone is given in Ch5 p57. Interpreted to have been deposited in a lacustrine environment. Sedimentary characteristics are briefly discussed. See also  Ch5 p57-p58, Ch7 p7-p8, Ch7 p13, Ch8 p5, Ch8 p10, Ch8 p17, Ch13 p4, Ch13 p9.||||Conformably overlies the Adori Sandstone. Conformably overlain by the Namur and Algebuckina Sandstones. This unit intertongues with, and is laterally equivalent to the Algebuckina Sandstone.|Interbedded darky grey shale and siltstone with minor sandstone interbeds.|
19796|Westbourne Formation|71806|6|Mentioned|p484|Jurassic|Jurassic|Surat Basin.||||||
19796|Westbourne Formation|71863|6|Mentioned|p5|Valanginian|Berriasian|NE Eromanga Basin. Shown as "uppermost Westbourne Formation".||||||
19796|Westbourne Formation|72297|6|Mentioned|p739, p742|||Eromanga Basin. Petroleum reservoir, with marginal source rock potential.||||||
19796|Westbourne Formation|72298|5|Briefly described|p801|Jurassic|Jurassic|Eromanga Basin (SA,QLD,NSW), Surat Basin (QLD,NSW).||Injune Creek Group.||Overlies Adori or Springbok Sandstone. Is overlain by Namur and Hooray Sandstones.||
19796|Westbourne Formation|72921|5|Briefly described|p15 Fig.2, p16.|Late Jurassic|Late Jurassic|Shown as located in the Surat Basin in Queensland and the Eromanga Basin.||||Overlies and is laterally equivalent to Adori Sandstone and underlies Namur Sandstone and Hooray Sandstone.|May include siltstone.|
19796|Westbourne Formation|73113|5|Briefly described|p. 22-24, 31, 36-37, 41, 49, 66-67...|||Surat Basin. Tight aquitard. More locations: p. 69, 71, 78, 80, 98, 115-116, 119, 128-129, 148-149, 152, 167, 169-172, 177-178, 191.||||Underlain by Springbok Sandstone. Overlain by Gubberamunda Sandstone.||
19796|Westbourne Formation|73167|6|Mentioned|p664 Fig. 2|Cretaceous|Jurassic|Eromanga Basin. Contains oil.||||||
19796|Westbourne Formation|73193|6|Mentioned|p369|Tithonian|Kimmeridgian|Surat Basin.||Injune Creek Group||Underlain by Springbok Sandstone. Unconformably overlain by Gubberamunda Sandstone.||
19796|Westbourne Formation|73200|6|Mentioned|p533|Jurassic|Jurassic|||||||
19796|Westbourne Formation|73251|6|Mentioned|p62|Late Jurassic|Late Jurassic|Eromanga Basin. Deposited in a braided-meandering fluvial setting. Oil show.||||Underlain by Adori Sandstone. Overlain by and equivalent to Namur Sandstone. Equivalent to Algebuckina Sandstone.||
19796|Westbourne Formation|73343|6|Mentioned|p337|Jurassic|Jurassic|Eromanga Basin. Hosts oil.||||Underlain by Adori Sandstone. Overlain by Hooray Sandstone.||
19796|Westbourne Formation|73393|6|Mentioned|p20-21|Tithonian|Tithonian|Surat and Eromanga Basins.||Injune Creek Group||Underlain by Adori Sandstone. Underlain by and equivalent to Springbok Sandstone.||
19796|Westbourne Formation|73479|5|Briefly described|p156 Fig.2, p159|Jurassic|Jurassic|Eromanga Basin. Braided fluvial-lacustrine depositional environment.|ca 150 Ma|||Overlies Adori Sandstone, underlies Hooray Sandstone||
19858|Whalers Bluff Formation|22944|5|Briefly described|Fig3|Pleistocene|Miocene|||||||
19858|Whalers Bluff Formation|23768|5|Briefly described|p27, p30 Fig.6, p185|Early Pleistocene|Late Pliocene|Overlies Werrikoo Limestone.  Age: <4.35Ma. Geological Province: Otway Basin.||||||
19858|Whalers Bluff Formation|23909|5|Briefly described|p291|Pliocene|Pliocene|Geological Province: Otway Basin.||||||
19858|Whalers Bluff Formation|24551|5|Briefly described|p338 Fig. 11.2, 342, 306|Early Pleistocene|Late Pliocene|Overlies: Heytesbury Group.||||||
19858|Whalers Bluff Formation|24562|6|Mentioned|p69 Fig. 27|||Geological Province: Otway Basin.||||||
19858|Whalers Bluff Formation|29355|6|Mentioned|p185|||||||||
19858|Whalers Bluff Formation|30393|6|Mentioned|p309|||||||||
19858|Whalers Bluff Formation|30865|6|Mentioned|p306|||Upper Pliocene-Lower Pleistocene||||||
19858|Whalers Bluff Formation|30928|6|Mentioned|Map legend|Quaternary|Quaternary|||||||
19858|Whalers Bluff Formation|30932|6|Mentioned|Map legend|Pliocene|Pliocene|||||||
19858|Whalers Bluff Formation|31036|6|Mentioned|Table 9-1|||Pliocene||||||
19858|Whalers Bluff Formation|31345|6|Mentioned|FigXIII-47|||||||||
19858|Whalers Bluff Formation|31372|4|Described|p10|||||||||
19858|Whalers Bluff Formation|31424|6|Mentioned|p13|||||||||
19858|Whalers Bluff Formation|31624|4|Described|p98|||See also p127, 128. L.Pleistocene.||||||11-AUG-15
19858|Whalers Bluff Formation|31625|6|Mentioned|Fig. 5.2|||Pleistocene||||||
19858|Whalers Bluff Formation|31628|6|Mentioned|Map legend|Pleistocene|Pleistocene|Enclosure 5-4||||||
19858|Whalers Bluff Formation|31629|6|Mentioned|Fig. 5.1|||L.Pleistocene||||||
19858|Whalers Bluff Formation|32767|6|Mentioned|p66|||||||||
19858|Whalers Bluff Formation|33160|4|Described|p302|||||||||
19858|Whalers Bluff Formation|34832|6|Mentioned|p23|||||||||
19858|Whalers Bluff Formation|34954|5|Briefly described|p198|||||||||
19858|Whalers Bluff Formation|34988|6|Mentioned|p290|||||||||
19858|Whalers Bluff Formation|35066|3|Fully described|p217|||||||||
19858|Whalers Bluff Formation|35097|6|Mentioned|p30|||||||||
19858|Whalers Bluff Formation|35271|6|Mentioned|Fig.2|||||||||
19858|Whalers Bluff Formation|35274|6|Mentioned|p424|||||||||
19858|Whalers Bluff Formation|35722|6|Mentioned|p4|||Stratigraphy.||||||
19858|Whalers Bluff Formation|36366|6|Mentioned|p5|||||||||
19858|Whalers Bluff Formation|37399|6|Mentioned|Fig.1|||||||||
19858|Whalers Bluff Formation|37548|6|Mentioned|p131|||||||||
19858|Whalers Bluff Formation|38070|6|Mentioned|Fig.12|||Otway Basin||||||
19858|Whalers Bluff Formation|39077|6|Mentioned|p25|||||||||
19858|Whalers Bluff Formation|40230|6|Mentioned|Fig.1|||||||||
19858|Whalers Bluff Formation|40643|6|Mentioned|p155|||||||||
19858|Whalers Bluff Formation|41043|6|Mentioned|p98|||||||||
19858|Whalers Bluff Formation|41185|6|Mentioned|Fig.4|||||||||
19858|Whalers Bluff Formation|41521|6|Mentioned|p240|||||||||
19858|Whalers Bluff Formation|41599|6|Mentioned|p192|||||||||
19858|Whalers Bluff Formation|41642|6|Mentioned|Fig.8.6|||||||||
19858|Whalers Bluff Formation|41704|6|Mentioned|Fig.3|||||||||
19858|Whalers Bluff Formation|41769|6|Mentioned|p50|||||||||
19858|Whalers Bluff Formation|41848|5|Briefly described|p365|||see Ch8 p291 for description Age Plio-Pleistocene||||||
19858|Whalers Bluff Formation|41868|5|Briefly described|p578|||||||||
19858|Whalers Bluff Formation|42524|5|Briefly described|Fig.3 P27|||||||||
19858|Whalers Bluff Formation|42635|5|Briefly described|p91|||||||||
19858|Whalers Bluff Formation|42827|2|Defined|p291|early Pleistocene|late Pliocene|see also Fig 8.9||||||
19858|Whalers Bluff Formation|42863|5|Briefly described|Fig.14|||Variation on Victorian unit.||||||
19858|Whalers Bluff Formation|43660|6|Mentioned|Fig.6,p15|Pleistocene|Miocene|||||||
19858|Whalers Bluff Formation|46802|6|Mentioned|Table 1|||||||||
19858|Whalers Bluff Formation|48911|6|Mentioned|p29|||See also Chart 1||||||
19858|Whalers Bluff Formation|48925|6|Mentioned|p13|||Upper Pliocene age. Fauna. P25 etc.||||||
19858|Whalers Bluff Formation|50154|2|Defined|p26, p139|Pliocene|Pliocene|Considered to be offshore equivalent of Parilla Sand. Predominantly of Pliocene age. Max. thickness: 35m. Disconformably overlies the Murray Group and Otway Group.||||||15-SEP-04
19858|Whalers Bluff Formation|50155|5|Briefly described|Map Legend|Pleistocene|Miocene|Limestone, marl||||||
19858|Whalers Bluff Formation|50156|5|Briefly described|Map Legend|Pleistocene|Miocene|Coastal: sandy limestone, calcarenite, shell beds, marl||||||
19858|Whalers Bluff Formation|50157|5|Briefly described|Map Legend|Pleistocene|Miocene|Overlain by Bridgewater Formation and Lowan Sand Coastal: sandy limestone, calcarenite, shell beds, marl.||||||07-APR-09
19858|Whalers Bluff Formation|50158|5|Briefly described|Map Legend|Pleistocene|Miocene|Coastal: sandy limestone, calcarenite, shell beds, marl.||||||07-APR-09
19858|Whalers Bluff Formation|50159|5|Briefly described|Map Legend|Pleistocene|Miocene|Coastal: sandy limestone, calcarenite, shell beds, marl||||||
19858|Whalers Bluff Formation|50160|5|Briefly described|Map Legend|Pleistocene|Miocene|Sandy limestone, calcarenite, shell beds.||||||07-APR-09
19858|Whalers Bluff Formation|50161|5|Briefly described|Map Legend|Pleistocene|Miocene|Coastal: sandy limestone, calcarenite, shell beds, marl||||||
19858|Whalers Bluff Formation|50162|5|Briefly described|Map Legend|Pleistocene|Miocene|Coastal: sandy limestone, calcarenite, shell beds, marl||||||
19858|Whalers Bluff Formation|50163|5|Briefly described|Map Legend|Pleistocene|Miocene|Coastal: sandy limestone, calcarenite, shell beds, marl||||||
19858|Whalers Bluff Formation|50164|5|Briefly described|Map Legend|Quaternary|Miocene|Limestone, marl.||||||
19858|Whalers Bluff Formation|60421|5|Briefly described|p417|Middle Pliocene|Early Pliocene|||||||
19858|Whalers Bluff Formation|60538|5|Briefly described|p471 Fig. 10|Pliocene|Pliocene|||||||
19858|Whalers Bluff Formation|60785|5|Briefly described|p184 Fig.1, p186, pp207-208.  |Zanclean|Zanclean|Of the Otway Basin. The nodule layer has yielded worn, isolated fossil cetacean elements. Written as Whaler's Bluff Formation in Fig.1.|||||Includes a basal phosphatic nodule bed, fossiliferous clays, oyster beds and sandy limestones.|
19858|Whalers Bluff Formation|61155|5|Briefly described|p18|Pleistocene|Late Pliocene|Relatively thin limestones, marls and clays. Thickness: 130m. Geological Province: Otway Basin. See also p5, p6.||||||
19858|Whalers Bluff Formation|61181|5|Briefly described|p135|Pleistocene|Pliocene|Sandy limestone and lime sand of shallow marine origin, containing oyster beds. Age of the limestone: probably Miocene-Pliocene. Thickness: up to 20m.||||||
19858|Whalers Bluff Formation|61624|5|Briefly described|p465, p466, p466 Fig. 2|Quaternary|Pliocene|Geological Province: Otway Basin. Equivalents of Hanson Plain Sand, Moorabool Viaduct Formation and Grangeburn Formation. Mixed clastic/carbonate sediments.||||||
19858|Whalers Bluff Formation|62068|5|Briefly described|p135, Fig.2|Pliocene|Pliocene|||||Overlies the Port Campbell and Portland Limestones. Overlain by the Werrikoo Limestone||
19858|Whalers Bluff Formation|62899|6|Mentioned|p42|Pleistocene|Late Pliocene|At Myaring Bridge in south west Victoria.||||||
19858|Whalers Bluff Formation|63446|5|Briefly described|Map legend|Pleistocene|Pleistocene||||||Coastal: sandy limestone, calcarenite, shell beds, marl.|
19858|Whalers Bluff Formation|63739|5|Briefly described|p42|Pleistocene|Late Pliocene|Contains ostracod specimens eg. Rotundracythere sp. at Myaring Bridge in south west Victoria.||||||01-JUL-08
19858|Whalers Bluff Formation|66002|6|Mentioned|p13 Tb.9|||Defined by Boutakoff and Sprigg 1953.||||||
19858|Whalers Bluff Formation|67061|6|Mentioned|p554 Fig.10.|Pliocene|Pliocene|Otway Basin.||||Is overlain by Werriko Limestone.||
19858|Whalers Bluff Formation|68116|5|Briefly described|Appendix, Maps 38, 47.|Pliocene|Pliocene||||||Bioclastic calcarenite with lenses of foraminiferal clay, shelly clay and marl; quartz sand near the base.|
19858|Whalers Bluff Formation|73357|6|Mentioned|p48|Pliocene|Pliocene|Otway Basin.||Of Whalers Bluff Group?||||
19865|Wheepool Rhyolite|22629|6|Mentioned|p158|Calymmian|Calymmian|||||||
19865|Wheepool Rhyolite|24474|4|Described|p40-41|Mesoproterozoic|Mesoproterozoic|Of the Glyde Hill Volcanic Complex.   Overlies Waurea Pyroclastics (named by Giles) which is included within Wheepool Rhyolite by Blissett (1980).  Max. thickness: 300m.  Geological Province: Gawler Craton.||||||
19865|Wheepool Rhyolite|29838|2|Defined|p12|Mesoproterozoic|Mesoproterozoic|||||||
19865|Wheepool Rhyolite|30984|6|Mentioned|p11|||||||||
19865|Wheepool Rhyolite|41974|6|Mentioned|Fig.1 P408|||||||||
19865|Wheepool Rhyolite|42546|5|Briefly described|Map legend|Mesoproterozoic||||||||
19865|Wheepool Rhyolite|42721|5|Briefly described|map legend|Carpentarian||||||||
19865|Wheepool Rhyolite|42722|5|Briefly described|map legend|Carpentarian|Carpentarian|Of the Glyde Hill Volcanic Complex.  Yellowich-brown weathered, reddish-brown prophyritic rhyolite, grading to rhyodacite localy; phenocrysts of pink K-feldspar and ronded quartz.||||||07-APR-05
19865|Wheepool Rhyolite|42736|5|Briefly described|map legend|Mesoproterozoic||||||||
19865|Wheepool Rhyolite|43052|5|Briefly described|p111|||of Glyde Hill Volcanics Complex||||||
19865|Wheepool Rhyolite|43071|5|Briefly described|p14,Table 2|||of Gawler Range Volcanics||||||
19865|Wheepool Rhyolite|43094|4|Described|Table 4.|||of Glyde Hill Volcanic Complex||||||
19865|Wheepool Rhyolite|67909|5|Briefly described|p126-129, 132-134, 136-137, 139|Mesoproterozoic|Mesoproterozoic|Lake Everard area. Volcanic textures and emplacement mechanism tabulated. Contains well-preserved quartz-phenocryst-hosted melt inclusions (experiments detailed).||Glyde Hill Volcanic Complex.|||Massive or flow-banded porphyritic lavas.|
19865|Wheepool 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.|
19865|Wheepool Rhyolite|70816|5|Briefly described|p5|||Lake Everard area, Gawler Ranges.||Unit of Glyde Hill Volcanic Complex.||Overlain by Waurea Pyroclastics. Underlain by Arburee Rhyolite.||
19865|Wheepool Rhyolite|72090|6|Mentioned|p12|||Gawler Craton.||Glyde Hill Volcanic Complex||||
19868|Whidbey Granite|22489|6|Mentioned|p14|Archean|Archean|||||||07-NOV-08
19868|Whidbey Granite|22629|5|Briefly described|p148|||||||||
19868|Whidbey Granite|33727|4|Described|p35|||Incl. dating||||||
19868|Whidbey Granite|37373|6|Mentioned|p36|||||||||
19868|Whidbey Granite|37620|6|Mentioned|p8|||||||||
19868|Whidbey Granite|37811|6|Mentioned|Fig.3|||||||||
19868|Whidbey Granite|39352|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
19868|Whidbey Granite|39802|6|Mentioned|Map legend|Archean|Archean|||||||07-NOV-08
19868|Whidbey Granite|40448|5|Briefly described|Table 2|||||||||
19868|Whidbey Granite|40644|5|Briefly described|p120, p125, p126 Fig.5|Paleoproterozoic||Of Webb and Thomson (1977). Included in the Dutton suite as presented in this paper. Geological province: Gawler Craton. Massive, equigranular granite. Age: 2334+/-109Ma. See also  p124 Fig. 3, .||||||07-NOV-08
19868|Whidbey Granite|41667|6|Mentioned|p2|||||||||
19868|Whidbey Granite|43052|5|Briefly described|p38,Table 3.1|||Of Dutton Suite.||||||04-MAR-09
19868|Whidbey Granite|50605|5|Briefly described|p4.2, 8.7|||Geological Province: Gawler Craton & Curnamona Province. Of the Dutton Suite (Sleaford Complex).||||||
19868|Whidbey Granite|61070|5|Briefly described|Map Legend|Proterozoic|Archean|Of the Dutton Suite.  Grey-pink, equigranular, medium to coarse-grained granite.  Predomiantly massive, weakly foliated. Age: 2337 +/- 71Ma (Rb-Sr whole rock). Geological Province: Gawler Craton.||||||12-JAN-10
19868|Whidbey Granite|64828|5|Briefly described|p1065 Fig. 2|||Of the Dutton Suite. Included in the Sleaford Complex also. Age: 2445+/-4Ma (Jagodzinski et al 2006).||||||04-MAR-09
19868|Whidbey Granite|65376|5|Briefly described|p15.|||Has enclaves of Coulta Granodiorite.||Unit in Dutton Suite.|||Even-grained granite.|
19868|Whidbey Granite|66302|6|Mentioned|p14|||||Dutton Suite||||
19868|Whidbey Granite|71859|5|Briefly described|p9-p10|||Southern Eyre Peninsula.|c. 2440 Ma (Webb et al., 1986)|Dutton Suite|||K-feldspar, microcline, quartz, plagioclase and minor biotite granite.|06-APR-23
19901|White Point Conglomerate|5249|6|Mentioned|p31|Early Cambrian||Conformably underlies Emu Bay Shale at the latter's type section in Emu Bay.||||||
19901|White Point Conglomerate|6111|6|Mentioned|p23, p24 Fig.2|Early Cambrian|Early Cambrian|||||Underlies Emu Bay Shale, locally unconformably.||17-SEP-12
19901|White Point Conglomerate|22581|4|Described|Fig.2,p37|||Of the Kangaroo Island Group. Thickness: 550 m. Overlies Smith Bay Shale. Overlain by Emu Bay Shale||||||02-JUL-08
19901|White Point Conglomerate|22643|5|Briefly described|p186, fig3,6|Early Cambrian|Early Cambrian|||||||
19901|White Point Conglomerate|22766|4|Described|Fig.2 p561, p563|Early Cambrian|Early Cambrian|||||||
19901|White Point Conglomerate|22857|5|Briefly described|p88 Fig. 14.7A|Early Cambrian|Early Cambrian|Of the Kangaroo Island Group. Geological Province: Stansbury Basin.||||||
19901|White Point Conglomerate|22858|6|Mentioned|Fig14.7ap88-9|Toyonian|Toyonian|||||||
19901|White Point Conglomerate|23818|5|Briefly described|p87 Fig.33, p105|Cambrian|Cambrian|Of the Kangaroo Island Group. Max. thickness: 1000 ft.||||||
19901|White Point Conglomerate|23981|6|Mentioned|p22, p64|||Contains re-worked Koolywurtie-type reefal clasts. On Kangaroo Island. Together with Emu Bay Shale is correlated with Oraparinna Shale through trilobite similarities.||||||
19901|White Point Conglomerate|32669|6|Mentioned|p523|||L.Camb.||||||
19901|White Point Conglomerate|33332|6|Mentioned|p11|||L.Camb.||||||
19901|White Point Conglomerate|33471|6|Mentioned|Fig.1|||||||||
19901|White Point Conglomerate|34612|5|Briefly described|p105|||Lower Cambrian. See Fig.33||||||
19901|White Point Conglomerate|35255|6|Mentioned|Fig.8|||||||||
19901|White Point Conglomerate|35487|6|Mentioned|p21|||||||||
19901|White Point Conglomerate|35835|6|Mentioned|p209|||||||||
19901|White Point Conglomerate|36198|6|Mentioned|Fig.I.2|||||||||
19901|White Point Conglomerate|36495|6|Mentioned|p123|||||||||
19901|White Point Conglomerate|38873|4|Described|Table 3|||See also Fig.8||||||
19901|White Point Conglomerate|40856|6|Mentioned|Fig.23.6|||||||||
19901|White Point Conglomerate|41106|5|Briefly described|p168|||||||||
19901|White Point Conglomerate|41947|6|Mentioned|Fig.2 P17|||||||||
19901|White Point Conglomerate|42192|6|Mentioned|p15|||||||||
19901|White Point Conglomerate|42222|6|Mentioned|p21|||||||||
19901|White Point Conglomerate|42225|6|Mentioned|p221|||||||||
19901|White Point Conglomerate|42268|5|Briefly described|p325|||White Point Limestone of Sprigg 1955||||||12-JAN-10
19901|White Point Conglomerate|42269|6|Mentioned|Fig.1 P335|||||||||
19901|White Point Conglomerate|42272|5|Briefly described|p411|||||||||
19901|White Point Conglomerate|43190|5|Briefly described|Fig.1,p28.|||of Kangaroo Island Group.||||||
19901|White Point Conglomerate|44133|5|Briefly described|p4 Fig. 7.2, 6, p12|Early Cambrian|Early Cambrian|Geological Province: Stansbury Basin. Of the Kangaroo Island Group.||||||
19901|White Point Conglomerate|45102|6|Mentioned|p47|||||||||
19901|White Point Conglomerate|62270|5|Briefly described|p496, p502|Early Cambrian|Early Cambrian|Contains Emuellids (Trilobite family). On Kangaroo Island. Sree also p504 Fig. 3, p507 Fig. 6.||||||
19901|White Point Conglomerate|62785|6|Mentioned|p43, p44 Fig.1|Early Cambrian|Early Cambrian|North coast Kangaroo Island. Overlies Smith Bay Shale and unconformably underlies Emu Bay Shale.||||||20-MAR-12
19901|White Point Conglomerate|63569|6|Mentioned|p122|||Kangaroo Island||||||
19901|White Point Conglomerate|64282|5|Briefly described|Map legend|Early Cambrian|Early Cambrian|Of Kangaroo Island Group. Geological Province: Stansbury Basin. Very coarse, current bedded, polymict conglomerate, interbedded with red-brown micaceous shale , siltstone and gritty sandstone.  Abundantly bioturbated with syneresis and mud cracks.||||||24-JUL-08
19901|White Point Conglomerate|64829|5|Briefly described|p1086|Early Cambrian|Early Cambrian|On Kangaroo Island. A synorogenic alluvial fan with boulders up to 50cm diameter.||||||07-FEB-11
19901|White Point Conglomerate|65375|5|Briefly described|p33.|Early Cambrian|Early Cambrian|||Unit in Kangaroo Island Group.||Overlies Smith Bay Shale. Is overlain by Emu Bay Shale.||
19901|White Point Conglomerate|65625|4|Described|p124-125, 103|Early Cambrian|Early Cambrian|Previously White Point Limestone (Sprigg, 1954, 1955). Archaeocyathid limestone boulders common. Trilobites in shale near top of unit. Type locality 1 mile WSW of White Point. Thickness: ~1250ft.||Of Kangaroo Island Group.||Conformable over unnamed unit; conformable under Emu Bay Shale.|Polymictic conglomerates interbedded with shales and quartzites.|13-APR-11
19901|White Point Conglomerate|65667|5|Briefly described|p1222, p1223|Early Cambrian|Early Cambrian|||||Overlies Smith Bay Shale and underlies (unconformably in places) Emu Bay Shale.|Moderately well-sorted, thin-bedded to massive, feldspathic to arkosic fine to medium sandstones, granular and polymict conglomerates.|27-MAR-12
19901|White Point Conglomerate|65686|6|Mentioned|p411, 414|Early Cambrian|Early Cambrian|Kangaroo Island.|||||Contains shale horizons.|07-MAY-12
19901|White Point Conglomerate|65892|5|Briefly described|p9 Fig.4, p22, p24. |Early Cambrian|Early Cambrian|North Coast of Kangaroo Island. The sequence of clasts indicates progressive erosion of earlier Cambrian sediments (eg Koolywurtie Limestone on Yorke Peninsula) followed by basement rocks.||||Overlies Smith Bay Shale. Is overlain by Emu Bay Shale.|Red sandstone, minor siltstone and shale overlain by boulder conglomerate with sandstone matrix. Clasts include archaeocyath- or trilobite-bearing limestone, dolomite, sandstone, succeeded by gneisses and granites.|
19901|White Point Conglomerate|65921|6|Mentioned|p1, p2 (map legend).|Cambrian|Cambrian|Contains trilobites at Big Gully.||Of the Kangaroo Island Group.||||
19901|White Point Conglomerate|66761|4|Described|p244-249,252-254|Early Cambrian|Early Cambrian|605m thick along coast. Archaeocyaths in cobbles and boulders, so must post-date Mount McDonnell Formation.||Of Kangaroo Island Group.||Said to overlie Smith Bay Shale in Investigator 1.|Cross-bedded  cobble to boulder conglomerate, minor mudstone and sandstone.|14-MAR-12
19901|White Point Conglomerate|67344|5|Briefly described|p260 Fig.1, p261|Early Cambrian|Early Cambrian|560m thick.||||Conformably overlain by the Marsden Sandstone.|Cobble to boulder conglomerate, fining southwards to arkose with polymict conglomerate lenses.|
19901|White Point Conglomerate|69372|6|Mentioned|p27 fig. 5, p34 fig. 12|Cambrian|Cambrian|||Kangaroo Island Group|||Conglomerate.|
19901|White Point Conglomerate|73107|5|Briefly described|Map legend.|Early Cambrian|Early Cambrian|Stansbury Basin.|||||Very coarse, current-bedded, polymict conglomerate interbedded with red-brown micaceous shale, siltstone and gritty sandstone. Abundantly bioturbated with syneresis and mud cracks.|
19901|White Point Conglomerate|73247|5|Briefly described|p204-207, p209-210|||Part of the eastern succession of the Kangaroo Island Group. Contains poorly preserved hyoliths in a sandstone near the base. Also contains limestone boulder clasts with a rich assemblage of archaeocyaths.||Kangaroo Island Group||Overlain by Marsden Sandstone including Rouge Mudstone Member. Equivalent to Stokes Bay Sandstone and Kanmantoo Group.||
19901|White Point Conglomerate|75071|6|Mentioned|p213|Early Cambrian|Early Cambrian|Kangaroo Island.||||||
19936|Whitula Formation|23982|6|Mentioned|p97 Appendix 13|||Geological Province: Great Artesian Basin.||||||
19936|Whitula Formation|33078|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
19936|Whitula Formation|33079|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
19936|Whitula Formation|35793|6|Mentioned|Fig.2|||||||||
19936|Whitula Formation|37607|6|Mentioned|Fig.4|||||||||
19936|Whitula Formation|38226|6|Mentioned|Table 1|||||||||
19936|Whitula Formation|39445|5|Briefly described|Table 14|||||||||
19936|Whitula Formation|39478|6|Mentioned|Table 1|||||||||
19936|Whitula Formation|40739|6|Mentioned|p589|||||||||
19936|Whitula Formation|41198|6|Mentioned|Table 1|||||||||
19936|Whitula Formation|42375|5|Briefly described|Table 1 P11|||In Waite Basin. Previously used in Qld.||||||19-DEC-06
19936|Whitula Formation|42543|6|Mentioned|p6|||SA.||||||
19936|Whitula Formation|42746|6|Mentioned|p18|||||||||
19936|Whitula Formation|44041|6|Mentioned|Fig.1|||||||||
19936|Whitula Formation|44133|5|Briefly described|p190 Fig. 10.30|Early Pliocene|Late Miocene|||||||
19936|Whitula Formation|46802|6|Mentioned|Table 1|||||||||
19936|Whitula Formation|46854|6|Mentioned|Fig.1|||||||||
19936|Whitula Formation|46911|6|Mentioned|Fig.1|||Geological map and distribution of weathered profiles.||||||
19936|Whitula Formation|60080|5|Briefly described|Map legend|Pliocene|Miocene|Sandstone, siltstone, mudstone, and claystone, oxidised; minor gypsum and immature silcrete.  Overlies Glendower Formation; underlies Cadelga Limestone.||||||20-AUG-04
19936|Whitula Formation|61155|5|Briefly described|p17|Late Pliocene|Middle Miocene|Deposited in synclinal basins in southwest Queensland. Overlies the Cadelga Limestone. Age: 12-2Ma. Thickness: 220m. See also p4, p5.||||||
19936|Whitula Formation|64047|2|Defined|p61|Late Miocene|Late Miocene|Unconformably overlies Glendower Fm. or weathered Winton Fm. Overlain by Quaternary alluvium. Max. thickness: 160m. Contains interbedded quartzose sandstone, siltstone, mudstone and claystone with minor conglomerate; lignite and gypsum also present.||||||16-APR-08
19936|Whitula Formation|66131|6|Mentioned|p242 Fig.2, p245, p254|Miocene|Miocene|Senior and Mabbutt (1979) place the Cadelga Limestone and the Doonbara Formation at the top of this unit. Middle to Late Miocene in age (from Fig.2 - stratigraphic correlation chart).|||Includes Cadelga Limestone and Doonburra Formation.|||
19936|Whitula Formation|69599|5|Briefly described|p584, p599-602, p651|Miocene|Miocene|Senior et al. (1978). Eromanga, Lake Eyre Basins. Mostly known from drill holes. 53-160m thick. Fluviatile to lacustrine deposits. No fossils known. RELATED UNITS (continued): Also correlated (at least partly) with Horse Creek, Noranside, Austral Downs Limestones.||||Unconformably overlies Glendower and Winton Formations. Is overlain by Cadelga Limestone. Correlated with Doonbara, Poodyea Formations; and Mount Coley Sinter; see COMMENTS for more.|Interbedded quartzose sandstone, siltstone, mudstone and conglomerate; gypsiferous and lignitic in part.|
19936|Whitula Formation|70821|5|Briefly described|p25, p82|Miocene|Oligocene|Senior and Johnston (1974). Lake Eyre Basin (SA). Hydrostratigraphic properties.||||Equivalent to Namba Formation.||
19936|Whitula Formation|70823|5|Briefly described|p47|Pliocene|Late Oligocene|Maximum thickness of 160m.|ca 28 Ma||||Clay, fine-grained sand, carbonate and minor conglomerate.|17-SEP-18
19942|Whyalla Sandstone|22510|5|Briefly described|p40, Table1.|||Of the Yerelina Subgroup.  Age: Marinoan. Stuart Shelf.||||||13-OCT-04
19942|Whyalla Sandstone|22677|3|Fully described|p734, Fig.2 p735|Neoproterozoic|Neoproterozoic|See also Fig.1 p734, Fig.3 p736||||||
19942|Whyalla Sandstone|22829|6|Mentioned|P16|||||||||
19942|Whyalla Sandstone|23250|5|Briefly described|p1124 Fig.2||Cryogenian|Correlate of Olympic Formation and Elatina Formation (Umberatana Group).||||||
19942|Whyalla Sandstone|23913|4|Described|p108, p110 Fig. 2|Adelaidean|Adelaidean|Geological Province: Sturt Shelf.  Underlying Unit: Yudnapinna Beds"". Overlying Unit: Nuccaleena Formation. Of the Umberatana Group.||||||30-SEP-08
19942|Whyalla Sandstone|24362|5|Briefly described|p42|Adelaidean|Adelaidean|Overlies Pandurra Formation.||||||
19942|Whyalla Sandstone|24476|4|Described|p547 Fig. 4|Vendian|Vendian|Overlies the Yudnapinna Beds"". Overlain by the Nuccaleena Formaiton.  Geological Province: Stuart Shelf.||||||
19942|Whyalla Sandstone|30310|6|Mentioned|p9|||Geology regarding mineralisation||||||
19942|Whyalla Sandstone|30315|6|Mentioned|p1297|||||||||
19942|Whyalla Sandstone|30806|6|Mentioned|Fig.1|||||||||
19942|Whyalla Sandstone|30845|6|Mentioned|Fig.1|||||||||
19942|Whyalla Sandstone|31395|6|Mentioned|p66|||||||||
19942|Whyalla Sandstone|31541|6|Mentioned|p545|||||||||
19942|Whyalla Sandstone|31719|4|Described|p16|||Sulphide deposits in Marinoan||||||
19942|Whyalla Sandstone|33224|6|Mentioned|p35|||Re aquifer||||||
19942|Whyalla Sandstone|33479|6|Mentioned|Fig.1|||||||||
19942|Whyalla Sandstone|33564|6|Mentioned|Fig.8|||||||||
19942|Whyalla Sandstone|34319|5|Briefly described|p70|||||||||
19942|Whyalla Sandstone|35255|5|Briefly described|p10|||See also Fig.3.||||||
19942|Whyalla Sandstone|35298|6|Mentioned|Fig.1|||||||||
19942|Whyalla Sandstone|36185|6|Mentioned|Fig.9|||||||||
19942|Whyalla Sandstone|37461|6|Mentioned|Table 5.I|||||||||
19942|Whyalla Sandstone|37932|6|Mentioned|p546|||||||||
19942|Whyalla Sandstone|38581|4|Described|p254|||||||||
19942|Whyalla Sandstone|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Marinoan||||||
19942|Whyalla Sandstone|39352|6|Mentioned|Map legend|Adelaidean|Adelaidean|Marinoan||||||
19942|Whyalla Sandstone|39724|6|Mentioned|Fig.6|||||||||
19942|Whyalla Sandstone|40257|6|Mentioned|p288|||||||||
19942|Whyalla Sandstone|40448|5|Briefly described|p38|||||||||
19942|Whyalla Sandstone|41405|3|Fully described|p194|||Mention p166. Originally W.Member||||||14-APR-16
19942|Whyalla Sandstone|41667|6|Mentioned|Fig.3|||||||||
19942|Whyalla Sandstone|42088|5|Briefly described|p544|||See also Fig.2 p546.||||||14-APR-16
19942|Whyalla Sandstone|42167|6|Mentioned|Fig.2 P115|||||||||
19942|Whyalla Sandstone|42168|6|Mentioned|p121|||||||||
19942|Whyalla Sandstone|42222|6|Mentioned|p17|||||||||
19942|Whyalla Sandstone|42469|5|Briefly described|p22|||Marinoan (Adelaidian) of Umberatana Group||||||
19942|Whyalla Sandstone|42546|5|Briefly described|Map legend|Adelaidean (Marinoan)|Adelaidean (Sturtian)|||||||
19942|Whyalla Sandstone|42736|5|Briefly described|map legend|Neoproterozoic||||||||
19942|Whyalla Sandstone|43052|5|Briefly described|p190,Table 6.1|||||||||
19942|Whyalla Sandstone|43094|6|Mentioned|p35|||||||||
19942|Whyalla Sandstone|44934|5|Briefly described|Map Legend||Adelaidean|||||||
19942|Whyalla Sandstone|47004|6|Mentioned|p328|||||||||
19942|Whyalla Sandstone|47012|6|Mentioned|p332|||||||||
19942|Whyalla Sandstone|61732|6|Mentioned|p150|||Geological Province: Adelaide Rift Complex.||||||07-FEB-11
19942|Whyalla Sandstone|65376|6|Mentioned|p139.|||152m thick at Emmie Bluff prospect.||||Overlies Tapley Hill Formation. Is overlain by Tregolana Shale.||
19942|Whyalla Sandstone|70082|6|Mentioned|p2-10,16|Cryogenian|Cryogenian|Stuart Shelf. Reference section: (possibly? Not explicitly mentioned on p2) Mt Gunson Mine (S31.44278, E137.135350). Contains red beds and periglacial paleosols, correlable to Elatina Formation.||||||
19942|Whyalla Sandstone|70334|4|Described|p2,20,38,47,50-56,77,88|Neoproterozoic|Neoproterozoic|Geological province: Gawler Craton. Of Stuart Shelf. Does not outcrop on CULTANA but is exposed in AUGUSTA and CARIEWERLOO. Periglacial aeolian sands. Thickness: 15-70m on CULTANA. Generally quite coarse-grained in the northern Stuart Shelf, becoming finer-grained to the southern Stuart Shelf, and more difficult to distinguish with the underlying fine-grained Wilmington Formation. Basal conglomeratic beds contain clasts of felsic volcanics from the Gawler Range Volcanics, and sandstone, quartzite and carbonate clasts from Brighton Limestone. Contemporaneous with glacial-marine Elatina Formation. Also underlain by the Wilmington Formation and unconformably underlain by the Brighton Limestone or Tapley Hill Formation.||Unit of Yerelina Subgroup.||Contemporaneous with Elatina Formation. Overlain by Nuccalenna Formation. Underlain by Angepena Formation.|Yellow-grey to brown fine to gritty bimodal sandstone containing gritty and conglomeratic horizons and siltstone interbeds, basal conglomeratic beds.|14-OCT-19
19942|Whyalla Sandstone|70659|6|Mentioned|p10|Neoproterozoic|Neoproterozoic|||||||
19942|Whyalla Sandstone|70816|6|Mentioned|p3|Neoproterozoic|Neoproterozoic|Gawler Ranges region.||||||
19942|Whyalla Sandstone|70948|6|Mentioned|p974|Neoproterozoic|Neoproterozoic|Geological province: Gawler Craton.||||||
19942|Whyalla Sandstone|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). Age shown as Marinoan.||Umberatana Group||Shown as younger than Tapley Hill Formation and older than Tent Hill Formation.|Fine to coarse-grained sandstone, minor siltstone and conglomerate.|
19942|Whyalla Sandstone|71129|4|Described|p1,15-16,64,98,101,107,110-112,114|Cryogenian|Cryogenian|Of Stuart Shelf. Aeolian to fluval-deltaic to shallow marine sedimentation during Marinoan glacial period. Generally poorly exposed as intensively kaolinite-weathered rocks on SIX MILE HILL, but occurs extensively in the subsurface. See p118 for outcrop distribution and drillhole intersections. Silty-shaly intervals are correlable to Reynella Siltstone Member (Elatina Formation). Historically difficult to distinguish between Whyalla Sandstone and Yudnapinna Beds-Wilmington Formation/Upalinna Subgroup in the southwestern Stuart Shelf. Thickest intersection of drill core is 74m from MSDP02. Detrital zircon anaylsis indicate that Whyalla Sandstone is derived from Pandurra Formation. Does not contain evidence of glaciation compared to the correlative Elatina Formation. Correlable to Nuccaleena Formation cap carbonate, and other cap carbonate successions in Namibia and China via global chemo- and lithostratigraphic correlations. See also p116,118-127,138,141,208,210,225,227.|Between c. 645 and 635 Ma|Unit of Yerelina Subgroup.||Overlain unconformably by Tregolana Shale. Correlable with Elatina and Nuccaleena formations. Underlain by Wilyerpa Formation or Tapley Hill Formation or Brighton Limestone or Gawler Range Volcanics.|Reddish-brown sandstones with minor conglomeratic and silty-shaly portions; locally contains clasts of Pandurra Formation and Gawler Range Volcanics.|
19942|Whyalla Sandstone|71130|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|||Umberatana Group.|||Fine- to coarse-grained sandstone, minor siltstone and conglomerate.|
19942|Whyalla Sandstone|71131|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Age shown as Marinoan.||Umberatana Group.|||Fine- to coarse-grained sandstone, minor siltstone and conglomerate.|
19942|Whyalla Sandstone|71712|6|Mentioned|p411|Neoproterozoic|Neoproterozoic|||Unit of Umberatana or Wilpena groups.||||
19942|Whyalla Sandstone|71895|5|Briefly described|p10,  p20, APP4. p4, APP8. p201-p203|||Stuart Shelf. Spectral analysis is provided.||Umberatana Group||Overlies the Brighton Limestone.|Purple to red-grey, coarse-grained and bimodal sandstone with well-rounded quartz grains.|
19942|Whyalla Sandstone|72090|6|Mentioned|p34|||Gawler Craton.||||||
19942|Whyalla Sandstone|72247|5|Briefly described|p39-43|Neoproterozoic|Neoproterozoic|Of Adelaide Geosyncline. Initially identified by Jones (1909) and Wainwright (1914) in outcrop at the 'Bornite Workings', now known as West Lagoon deposit. Formally defined by Coats and Preiss (1987); new type section defined at Cattle Grid Mine at Mount Gunson, or alternatively the interval in the Woomera Bore between 239 and 341m (Coats and Preiss 1987).||||Overlain by Whyalla Sandstone. Underlain disconformably by Pandurra Formation. Transitional to Elatina Formation and Angepena Formation.||
19942|Whyalla Sandstone|73110|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic||||||Sandstone, coarse-grained, bimodal, with large-scale crossbedding, sand grains very well rounded, spherical.|
19942|Whyalla Sandstone|73226|6|Mentioned|p3|||Hosts a fluorite vein in drillhole HODD3 (SA Geodata drillhole 268313).|||||Includes massive medium-grained sandstone.|
19942|Whyalla Sandstone|73227|4|Described|p23-37|Neoproterozoic|Neoproterozoic|Stuart Shelf. Marinoan. Contains sediment-hosted, stratabound Cu sulfide deposits in the Mount Gunson district. Such deposits may be within the strata or at the basal boundary. Type section is at Cattle Grid Mine, Mount Gunson. Generally poorly exposed regionally. Largely contained within the TORRENS and PORT AUGUSTA map sheets. Sedimentary structures include large-scale cross-bedding. Variable colour from grey-white (reduced) to red (oxidised / hematite cemented) (see also Tonkin, 2007). Interfingering of this unit with Elatina Formation represents probable glaciomarine incursions into the otherwise terrestrial environment of the Stuart Shelf. Frosting is inferred to be caused by acid etching from warm fluids rather than from aeolian effects. Glaciofluvial or aeolian depositional environment [article includes detailed discussion on depositional environment]. Complex diagenesis [see article]. Sulfide mineralisation accompanied by fluorite and barite cement from reducing fluids. High porosity; permits increased fluid flow. Widespread silicification of the upper several metres in the Mount Gunson region; extent roughly matches area of reduced alteration. Fe leaching may have contributed to massive ironstone deposits along the western margin of Pernatty Lagoon where the formation pinches out against the Pernatty Upwarp.||Umberatana Group||Underlain by Tapley Hill Formation, unconformably by Pandurra Formation, and conformably by Yudnapinna beds. Overlain by Nuccaleena Formation. Equivalent to Elatina Formation.|Bimodal, lithic quartz sandstone, characterised by the extreme rounding of quartz grains in the coarse fraction and the presence of reddish coloured coarse lithic grains of probable felsic volcanic origin.|
19942|Whyalla Sandstone|73234|6|Mentioned|p6, p20-21|||Stuart Shelf, Six Mile Hill. Marinoan glaciation. Deposited in fluvial to marginal marine-deltaic environments. Gawler Craton dominated provenance.||Yerelina Subgroup, Umberatana Group||||
19942|Whyalla Sandstone|74367|5|Briefly described|p7 Fig.6, p8-9, p11, p16-17, p20, p22-24|Cryogenian|Cryogenian|Deposited during Marinoan Glaciation. Misspelt as 'Sandtstone'. Broad time equivalent with Elatina Formation. See also p14.|641+/-6 Ma LA-ICP-MS detrital zircon MDA|Yerelina Subgroup||||
19949|Whyeela Dacite|30984|2|Defined|p11|Proterozoic|Proterozoic|||||||
19949|Whyeela Dacite|41974|6|Mentioned|Fig.1 P408|||||||||
19949|Whyeela Dacite|42546|5|Briefly described|Map legend|Mesoproterozoic||||||||
19949|Whyeela Dacite|42721|5|Briefly described|map legend|Carpentarian||||||||
19949|Whyeela Dacite|42736|5|Briefly described|map legend|Mesoproterozoic||||||||
19949|Whyeela Dacite|43052|5|Briefly described|p111|||of Glyde Hill Volcanic Complex||||||
19949|Whyeela Dacite|43094|4|Described|Table 4|||of Glyde Hill Volcanic Complex.||||||
19949|Whyeela Dacite|67909|6|Mentioned|p126-127, 131|Mesoproterozoic|Mesoproterozoic|Lake Everard area. Total volume is up to 1 km3.||Glyde Hill Volcanic Complex.||||
19949|Whyeela Dacite|69649|5|Briefly described|p25|Mesoproterozoic|Mesoproterozoic|Up to 100m thick; confined to a semicircular structure ~8 km across on GAIRDNER map.||Youngest extrusive unit in Glyde Hill Volcanic Complex.||Conformably overlies Yantea Rhyodacite.||26-FEB-15
19949|Whyeela Dacite|70659|5|Briefly described|p7, p8|Mesoproterozoic|Mesoproterozoic|||Glyde Hill Volcanic Complex.|||Localised felsic lava flow with coherent core and autobrecciated margins; close to source vent.|
19949|Whyeela Dacite|70816|5|Briefly described|p5|||Lake Everard area, Gawler Ranges.||Unit of Glyde Hill Volcanic Complex.||Uppermost unit of the Glyde Hill Volcanic Complex. Underlain by Yantea Rhyolite.||
19949|Whyeela Dacite|72090|6|Mentioned|p12|||Gawler Craton.||Glyde Hill Volcanic Complex||||
19950|Whylie Member|31532|4|Described|Table 1|||||||||
19958|Wiabuna Formation|23342|5|Briefly described|28 Fig.1|Holocene|Pleistocene|||||||
19958|Wiabuna Formation|23719|4|Described|p31|||See also page 30 table 9. Underlying unit Pooraka Formation. Geological Province: Gawler Craton.||||||
19958|Wiabuna Formation|30756|2|Defined|p2|late Pleistocene|late Pleistocene|See also P4||||||
19958|Wiabuna Formation|30922|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
19958|Wiabuna Formation|35772|4|Described|Table 1|||||||||
19958|Wiabuna Formation|38605|6|Mentioned|Table 5|||||||||
19958|Wiabuna Formation|39349|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
19958|Wiabuna Formation|40448|5|Briefly described|p43|||||||||
19958|Wiabuna Formation|42466|5|Briefly described|Map Legend|||||||||
19958|Wiabuna Formation|42475|4|Described|p24|||||||||
19958|Wiabuna Formation|42716|5|Briefly described|Map legend|Pleistocene||||||||
19958|Wiabuna Formation|42722|5|Briefly described|map legend|Pleistocene|Pleistocene|Pale brownish calcareous silty sand, with soft earthy, rubbly and nodular carbonates of the Loveday Soil developed locally.||||||22-MAY-14
19958|Wiabuna Formation|42738|5|Briefly described|map legend|Quaternary||||||||
19958|Wiabuna Formation|43049|5|Briefly described|p27|||||||||
19958|Wiabuna Formation|43071|5|Briefly described|p17,Table 3|||||||||
19958|Wiabuna Formation|44133|5|Briefly described|p251|Quaternary|Quaternary|||||||
19958|Wiabuna Formation|44864|5|Briefly described|Map Legend||Pleistocene|||||||
19958|Wiabuna Formation|61070|5|Briefly described|Map Legend|Late Pleistocene|Middle Pleistocene|Thin, aeolian silty and clayey calcareous sand. Commonly draped by thin veneers of Holocene quartz sands. Overlies Bridgewater Formation. Reworked from or inland equivalent of Bridgewater Formation.||||||12-JAN-10
19958|Wiabuna Formation|61155|5|Briefly described|p17|Holocene|Late Pliocene|Age: <2Ma. Geological Province: Eucla Basin.||||||
19958|Wiabuna Formation|62893|6|Mentioned|Map Legend|||||||||
19958|Wiabuna Formation|65922|5|Briefly described|p25 Tb. 4, p27, 28, p32|Pleistocene|Pleistocene|Yellowish to reddish brown clayey sand and silt with local calcrete. Interfingers with Moornaba Sand. Forms the cores of dunes formed by Moornaba Sand. Small-scale quarrying for aggregate.||||||
19958|Wiabuna Formation|69649|5|Briefly described|p33|||Firman (1977). Forms a veneer draping crystalline basement; some remnant dunes still preserved. Type area 19km E of Penong. Supports cereal cropping.||||Overlies Bridgewater Formation.|Aeolian, pale brown, calcareous sands and silts.|
19958|Wiabuna Formation|70337|5|Briefly described|Map legend.|Pleistocene|Pleistocene||||||Silt to fine-grained sand, orange-brown, calcareous, conglomeratic in part. Aeolian.|
19958|Wiabuna Formation|70893|6|Mentioned|p3 fig 1b|Pleistocene|Pleistocene|||||||
19958|Wiabuna Formation|71317|6|Mentioned|p150|||||||Overlain by the Moornaba Sand.||
19958|Wiabuna Formation|73103|5|Briefly described|Map legend.|Pleistocene|Pleistocene||||||Silt to fine-grained sand, orange-brown, calcareous, conglomeratic in part. Aeolian.|
19958|Wiabuna Formation|73302|6|Mentioned|p34|Pleistocene|Pleistocene|||||||
20023|Wilgena Hill Jaspilite|22629|4|Described|fig2p147,153|Statherian|Statherian|U-Pb geochronology on rhyolite in Labyrinth Formation: 1723+/-10Ma. Wilgena Hill Jaspilite occurs as fragments in this overlying unit, and is shown as significantly older in Figure 2 (~1850 Ma), suggesting age is poorly constrained.||||||29-APR-20
20023|Wilgena Hill Jaspilite|22851|5|Briefly described|12|Paleoproterozoic|Paleoproterozoic|Geol province Gawler Craton. Max thickness 1000 m||||||07-NOV-08
20023|Wilgena Hill Jaspilite|22854|6|Mentioned|p9||Paleoproterozoic|||||||29-APR-20
20023|Wilgena Hill Jaspilite|23124|5|Briefly described|p397|||||||||
20023|Wilgena Hill Jaspilite|23731|6|Mentioned|p11|||Geological Province: Gawler Craton.||||||
20023|Wilgena Hill Jaspilite|24472|5|Briefly described|p5 Tb.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Harris Greenstone Domain, Gawler Craton.||||||07-NOV-08
20023|Wilgena Hill Jaspilite|34904|6|Mentioned|p148|||||||||
20023|Wilgena Hill Jaspilite|36003|5|Briefly described|p1027|||||||||
20023|Wilgena Hill Jaspilite|39905|6|Mentioned|Fig.4|||||||||
20023|Wilgena Hill Jaspilite|42465|5|Briefly described|Map Legend|||||||||
20023|Wilgena Hill Jaspilite|42469|4|Described|p11|||||||||
20023|Wilgena Hill Jaspilite|43052|5|Briefly described|p68|||||||||
20023|Wilgena Hill Jaspilite|43053|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Iron formation.||||||07-NOV-08
20023|Wilgena Hill Jaspilite|43258|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
20023|Wilgena Hill Jaspilite|43298|6|Mentioned|Map Legend||Paleoproterozoic|||||||07-NOV-08
20023|Wilgena Hill Jaspilite|44935|5|Briefly described|Map Legend||Proterozoic|||||||
20023|Wilgena Hill Jaspilite|50605|6|Mentioned|p8.8|||||||||
20023|Wilgena Hill Jaspilite|60953|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
20023|Wilgena Hill Jaspilite|61108|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
20023|Wilgena Hill Jaspilite|61556|6|Mentioned|p8|||Stated that this unit resembles the Upper Haematite Quartzites  (Miles 1955) of the Middleback Ranges. See also Figure on p9-10.||||||21-NOV-07
20023|Wilgena Hill Jaspilite|63067|5|Briefly described|p2 Fig. 1|Paleoproterozoic|Paleoproterozoic|Age: >1740Ma. Banded iron formation, chert, quartzite.||||||07-NOV-08
20023|Wilgena Hill Jaspilite|63866|5|Briefly described|p17|||||||Overlies the Mulgathing Complex. Overlain by the Tarcoola Formation.|Fine-grained, finely laminated BIF.|
20023|Wilgena Hill Jaspilite|65376|6|Mentioned|p127 Fig.4.6.|Paleoproterozoic|Paleoproterozoic|||||||
20023|Wilgena Hill Jaspilite|65390|6|Mentioned|p22 Fig. 3|||Wilgena Domain, Gawler Craton.||||||
20023|Wilgena Hill Jaspilite|66302|5|Briefly described|p22, p32|Statherian|Statherian|Wilgena Domain, Gawler Craton.  In Fig.20, is grouped as Eba, Wilgena Hill and Labyrinth Fms.|ca. 1740-1710 Ma|||Overlies the Mulgathing Complex.|Finely-banded, red-black jaspilitic banded iron formation.|
20023|Wilgena Hill Jaspilite|67058|5|Briefly described|p479 Fig. 3|Paleoproterozoic|Paleoproterozoic|Gawler Craton|||||Jaspilite, banded iron formation|19-APR-12
20023|Wilgena Hill Jaspilite|67536|6|Mentioned|Map Legend|||Gawler Craton.|Unknown age.|||||
20023|Wilgena Hill Jaspilite|73233|6|Mentioned|p27 Fig.1|Paleoproterozoic|Paleoproterozoic|||||||
20023|Wilgena Hill Jaspilite|73235|6|Mentioned|p53, p58|||Gawler Craton. Wilgena and Harris Greenstone regions. No reliable age has been determined.||||||
20045|Wilkawillina Limestone|22650|6|Mentioned|p 159|Cambrian|Cambrian|Province - Adelaide Geosyncline.||||||
20045|Wilkawillina Limestone|22651|6|Mentioned|p 191|||Province - Flinders Ranges SA.||||||
20045|Wilkawillina Limestone|22652|6|Mentioned|p 196|||||||||
20045|Wilkawillina Limestone|22688|6|Mentioned|127,128|||||||||
20045|Wilkawillina Limestone|22766|5|Briefly described|Fig.2 p561|Early Cambrian|Early Cambrian|||||||
20045|Wilkawillina Limestone|23211|6|Mentioned|Fig.2|||of Hawker Group.||||||
20045|Wilkawillina Limestone|23287|6|Mentioned|Fig.2,4||Cambrian|of Adelaide Geosyncline.||||||02-MAY-13
20045|Wilkawillina Limestone|23818|4|Described|p87 Fig.33, p90|Cambrian|Cambrian|Of the Hawker Group. Underlying unit: Parachilna Formation. Contains abundant Archaecyatha.||||||
20045|Wilkawillina Limestone|23825|5|Briefly described|p254|Early Cambrian|Early Cambrian|Geological Province: Arrowie Basin.||||||
20045|Wilkawillina Limestone|23826|6|Mentioned|p95|||Geological Province: Arrowie Bain.||||||
20045|Wilkawillina Limestone|23981|5|Briefly described|p8-9 Fig. 4|Early Cambrian|Early Cambrian|Geological Province: Arrowie Basin.||||||04-FEB-08
20045|Wilkawillina Limestone|24072|5|Briefly described|p369 Fig.1|Cambrian|Cambrian|Geological Province: Great Artesian Basin.||||||
20045|Wilkawillina Limestone|24138|4|Described|p29|Cambrian|Cambrian|Frequently referred to as the Archaeocyatha Limestone. Sandy and shaly beds with fossil algae. Geological Province: Adelaide Geosyncline.||||||17-JUN-05
20045|Wilkawillina Limestone|24176|4|Described|p16-17, p23 Tb. 1|Cambrian|Cambrian|Massive grey limestone.  Intertongues with the Parara Limestone.  Geological Province: Mount Painter Province.||||||
20045|Wilkawillina Limestone|24281|5|Briefly described|p7|Early Cambrian|Early Cambrian|||||||
20045|Wilkawillina Limestone|24465|5|Briefly described|p345 Fig.2|Early Cambrian|Early Cambrian|Of the Hawker Group.  Geological Province: Arrowie Basin.||||||19-JAN-05
20045|Wilkawillina Limestone|24481|5|Briefly described|p828|||Of the Ajax Limestone.||||||
20045|Wilkawillina Limestone|24484|4|Described|p798 Fig.1, p804|Cambrian|Cambrian|Divided into Lower and Upper units by a regional unconformity. Overlies the Woodendinna Dolomite. Overlain by the Billy Creek Formation.||||||
20045|Wilkawillina Limestone|29780|6|Mentioned|p47|||||||||
20045|Wilkawillina Limestone|29929|6|Mentioned|p223|||||||||
20045|Wilkawillina Limestone|30051|6|Mentioned|p20|||||||||
20045|Wilkawillina Limestone|30176|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
20045|Wilkawillina Limestone|30198|4|Described|p97|||||||||
20045|Wilkawillina Limestone|30374|6|Mentioned|p29|||||||||
20045|Wilkawillina Limestone|30801|6|Mentioned|p5|||Lower Cambrian. Table P5-6||||||
20045|Wilkawillina Limestone|30802|5|Briefly described|p11|||Cambrian.||||||
20045|Wilkawillina Limestone|30807|6|Mentioned|p102|||Suggested map symbol||||||
20045|Wilkawillina Limestone|31022|4|Described|Fig. 4|||||||||
20045|Wilkawillina Limestone|31344|5|Briefly described|p2|||||||||
20045|Wilkawillina Limestone|31536|6|Mentioned|p10|||||||||
20045|Wilkawillina Limestone|31539|6|Mentioned|Fig. 8|||See also Fig. 9, 11, 17, 24, 22, 28.||||||
20045|Wilkawillina Limestone|31706|6|Mentioned|p633|||Cambrian correlation chart||||||
20045|Wilkawillina Limestone|31729|6|Mentioned|p111|||Geological map||||||
20045|Wilkawillina Limestone|31730|6|Mentioned|p99|||Geochem. Stream Sediment sampling.||||||
20045|Wilkawillina Limestone|31797|6|Mentioned|Fig. 2|||L.Camb. of Hawker Gp.||||||
20045|Wilkawillina Limestone|32504|6|Mentioned|Fig.2|||||||||
20045|Wilkawillina Limestone|32720|6|Mentioned|Table 1|||Hawker Group||||||
20045|Wilkawillina Limestone|32722|6|Mentioned|Fig.3|||L.Camb.||||||
20045|Wilkawillina Limestone|33474|6|Mentioned|Fig.3|||||||||
20045|Wilkawillina Limestone|33655|6|Mentioned|p87|||||||||
20045|Wilkawillina Limestone|33932|4|Described|p14|||||||||
20045|Wilkawillina Limestone|33934|4|Described|Fig.2|||L.Camb.||||||
20045|Wilkawillina Limestone|33954|6|Mentioned|p101|||||||||
20045|Wilkawillina Limestone|33973|6|Mentioned|p18|||||||||
20045|Wilkawillina Limestone|34122|6|Mentioned|p301|||Lower Cambrian||||||
20045|Wilkawillina Limestone|34202|6|Mentioned|p1058|||Hawker Group.||||||
20045|Wilkawillina Limestone|34267|6|Mentioned|Fig.|||The Oraparinna & Enorama diapiric structures.||||||
20045|Wilkawillina Limestone|34269|6|Mentioned|Table 1|||||||||
20045|Wilkawillina Limestone|34612|5|Briefly described|p90|||Lower Cambrian. See Fig.33||||||
20045|Wilkawillina Limestone|35075|6|Mentioned|p77|||||||||
20045|Wilkawillina Limestone|35255|6|Mentioned|Fig.8|||||||||
20045|Wilkawillina Limestone|35373|6|Mentioned|Fig.2|||||||||
20045|Wilkawillina Limestone|35395|5|Briefly described|p102|||Stratigraphy||||||
20045|Wilkawillina Limestone|35577|6|Mentioned|p3|||||||||
20045|Wilkawillina Limestone|35798|6|Mentioned|p311|||||||||
20045|Wilkawillina Limestone|35835|6|Mentioned|p201|||||||||
20045|Wilkawillina Limestone|36198|6|Mentioned|Fig.I.2|||||||||
20045|Wilkawillina Limestone|36495|6|Mentioned|p118|||||||||
20045|Wilkawillina Limestone|36525|6|Mentioned|Fig.4|||See also Fig.5.||||||
20045|Wilkawillina Limestone|36731|6|Mentioned|p125|||||||||
20045|Wilkawillina Limestone|37802|6|Mentioned|Fig.2|||||||||
20045|Wilkawillina Limestone|38068|5|Briefly described|p69|||||||||
20045|Wilkawillina Limestone|39675|6|Mentioned|p180|||||||||
20045|Wilkawillina Limestone|39904|6|Mentioned|p11|||||||||
20045|Wilkawillina Limestone|40431|4|Described|p12|||||||||
20045|Wilkawillina Limestone|40455|6|Mentioned|Fig.2|||||||||
20045|Wilkawillina Limestone|40642|6|Mentioned|p163|||||||||
20045|Wilkawillina Limestone|40672|6|Mentioned|p2|||||||||
20045|Wilkawillina Limestone|40831|6|Mentioned|p2|||||||||
20045|Wilkawillina Limestone|40852|6|Mentioned|p32|||||||||
20045|Wilkawillina Limestone|40856|6|Mentioned|Fig.23.6|||||||||
20045|Wilkawillina Limestone|40914|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
20045|Wilkawillina Limestone|40994|6|Mentioned|p266|||||||||
20045|Wilkawillina Limestone|40998|6|Mentioned|p441|||||||||
20045|Wilkawillina Limestone|41457|6|Mentioned|p1|||||||||
20045|Wilkawillina Limestone|41496|4|Described|p52|||||||||
20045|Wilkawillina Limestone|41526|6|Mentioned|p11|||||||||
20045|Wilkawillina Limestone|41996|6|Mentioned|p3|||||||||
20045|Wilkawillina Limestone|42011|5|Briefly described|p457|||||||||
20045|Wilkawillina Limestone|42090|6|Mentioned|p26|||||||||
20045|Wilkawillina Limestone|42095|5|Briefly described|Fig.3 P31|||||||||
20045|Wilkawillina Limestone|42192|6|Mentioned|p6|||||||||
20045|Wilkawillina Limestone|42213|5|Briefly described|p471|||See also Fig.1||||||
20045|Wilkawillina Limestone|42222|5|Briefly described|p20|||||||||
20045|Wilkawillina Limestone|42225|6|Mentioned|Fig.4 P224|||||||||
20045|Wilkawillina Limestone|42226|5|Briefly described|Fig.7 P241|||||||||
20045|Wilkawillina Limestone|42233|3|Fully described|p249|||See also Fig.2||||||
20045|Wilkawillina Limestone|42266|6|Mentioned|p299|||||||||
20045|Wilkawillina Limestone|42267|6|Mentioned|p314|||||||||
20045|Wilkawillina Limestone|42440|6|Mentioned|p605|||||||||
20045|Wilkawillina Limestone|42444|5|Briefly described|Fig.2 P16|||||||||
20045|Wilkawillina Limestone|42469|6|Mentioned|p25|||||||||
20045|Wilkawillina Limestone|42573|5|Briefly described|Fig.2 P191|||||||||
20045|Wilkawillina Limestone|43052|5|Briefly described|Table 2.1|||||||||
20045|Wilkawillina Limestone|43650|6|Mentioned|Fig.2,p444|||||||||
20045|Wilkawillina Limestone|43781|6|Mentioned|p4||Early Cambrian|||||||
20045|Wilkawillina Limestone|43845|6|Mentioned|Fig4 p44|||||||||12-JUL-16
20045|Wilkawillina Limestone|44133|5|Briefly described|p3, 22|Botomian||Conformably overlies: Parachilna Formation.||||||
20045|Wilkawillina Limestone|44659|5|Briefly described|map legend||Early Cambrian|L.Cambrian, lithology.||||||
20045|Wilkawillina Limestone|45102|6|Mentioned|p46|||||||||
20045|Wilkawillina Limestone|46957|6|Mentioned|p165|||||||||
20045|Wilkawillina Limestone|60418|5|Briefly described|p135|Early Cambrian|Early Cambrian|Of the Hawker Group. Overlain by Mernnerna Formation. Geological Province: Arrowie Basin of Adelaide Geosyncline.||||||
20045|Wilkawillina Limestone|60565|5|Briefly described|p18|Early Cambrian|Early Cambrian|Carbonates. Geological Province: Arrowie Basin.||||||
20045|Wilkawillina Limestone|60889|4|Described|p247, p249, p253-4|Early Cambrian|Early Cambrian|Biostratigraphy is discussed. Waxy paraffinic crude was found in carbonate cores in Wilkatana-1.||Hawker Group|||Karstic. Consists of archaeocyathan bioherms (in LD97-1).|
20045|Wilkawillina Limestone|60959|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of the Hawker Group. Light to dark grey, massive, bedded lime mudstone, wackestone, grainstone.||||||
20045|Wilkawillina Limestone|60990|5|Briefly described|p83 Fig.2, p83, p85|Botoman|Atdbanian|Wilkawillina Gorge, Arrowie Basin.  Biogeographic correlation with Cymbric Vale Formation. Faunal links with Antarctica.||Hawker Group.||||
20045|Wilkawillina Limestone|61308|5|Briefly described|p7|Cambrian|Cambrian|Sandy limestone.||||||
20045|Wilkawillina Limestone|61565|5|Briefly described|p609 Fig. 3|Cambrian|Cambrian|Geological Province: Adelaide Fold Belt.||||||26-MAY-06
20045|Wilkawillina Limestone|62570|6|Mentioned|p582|||Correlates with Ouldburra Formation in Offcier Basin.  Geological Province: Arrowie Basin.||||||
20045|Wilkawillina Limestone|62592|5|Briefly described|p50 Table 5.1|Early Cambrian|Early Cambrian|Adelaide Geosyncline.||Unit in Hawker Group.||Overlies Wirrapowie Limestone. Is overlain by Mern Merna Formation.|Archaeocyathan limestone.|
20045|Wilkawillina Limestone|62784|5|Briefly described|p8 Fig.1, p10 Fig. 3|Cambrian|Cambrian|Arrowie Basin. Unit in Hawker Group. Includes Second Plain Creek Member. Is unconformably overlain by Mernmerna Formation.||||||
20045|Wilkawillina Limestone|63447|5|Briefly described|p961, p962, p963, Fig.2|Early Cambrian|Early Cambrian|Upper part and lower part discussed seperately and shown as separate units in Fig. 2. Shallow water sediments.  Bioherm complexes form major part of unit.||Hawker Group||Upper part is laterally equivalent to the Moorowie Formation. Lower part laterally equivalent to Wirrapowie Limestone.|Generally consists of platform-derived archaeocyathan-calci-microbe limestone with a predominance of rubbly and argillaceous limestone.|
20045|Wilkawillina Limestone|63569|5|Briefly described|pp116-122, p138|Cambrian|Cambrian|Arrowie Basin, Adelaide Geosyncline. Contains trilobite taxa from the Abadiella huoi Zone.||Unit in Hawker Group.|Includes Second Plain Creek Member.|Is overlain unconformably by Mernmerna Formation; contact is the red microstromatolite horizon of the Flinders Unconformity.||
20045|Wilkawillina Limestone|64813|5|Briefly described|p272|Early Cambrian|Early Cambrian|Geological province: Arrowie Basin, S.A. Marine dolomitic limestones.||||||
20045|Wilkawillina Limestone|64829|5|Briefly described|p1084-5 Figs.1,  2|Early Cambrian|Early Cambrian|Unit discussed in the context of soilscapes and palaeosols. Contains marine archaeocyathids and shows local red breccias and paleokarst features created during exposure and dissolution.||||||07-FEB-11
20045|Wilkawillina Limestone|65313|6|Mentioned|p576 Fig. 5, p578 Fig. 6|Early Cambrian|Early Cambrian|~200 degrees burial temperature.||Of Hawker Group.||||26-MAR-12
20045|Wilkawillina Limestone|65625|5|Briefly described|p103 Fig.2|Early Cambrian|Early Cambrian|Lake Frome area.||||Overlies Pound Sandstone. Underlies Parara Limestone.||18-FEB-11
20045|Wilkawillina Limestone|65686|5|Briefly described|p413, p409 Fig 2, p412|Early Cambrian|Early Cambrian|Arrowie Basin.||||Underlies the Bunkers Sandstone.||07-MAY-12
20045|Wilkawillina Limestone|65892|4|Described|p7 Fig.3, p8, p10, p12, p29 Fig.14. |Early Cambrian|Early Cambrian|See also p38-39, p44, p46-48. Arrowie Basin. Platformal carbonates, including archaeocyathid-rich biohermal complexes. Described in some detail.|c.530 Ma.|Unit in Hawker Group.||Overlies Woodendinna Dolomite. Is locally interbedded with Mernmerna Formation.|Reefal limestone.|
20045|Wilkawillina Limestone|65925|5|Briefly described|p14 Fig.2.2, Appendix 2.|Early Cambrian|Early Cambrian||||||Archaeocyath-calcimicrobe limestone.|
20045|Wilkawillina Limestone|66518|6|Mentioned|p19 Fig.4.|Cambrian|Cambrian|Arrowie Basin.||Unit in Hawker Group.||Unconformably underlies Mernmerna Formation.||
20045|Wilkawillina Limestone|66623|6|Mentioned|p443.|||Arrowie Basin. Lower and upper parts separated by the Flinders unconformity. An unzoned interval between this and the Syringocnema favus beds is correlated with Mount Wright Volcanics of Koonenberry Belt.||||||
20045|Wilkawillina Limestone|67344|6|Mentioned|p264 Tb.3, p266 |Cambrian|Cambrian|Of the Arrowie Basin. Unmetamorphosed Cambrian series 2 formation. Shallow-water marine carbonate deposit. Bulk organic carbon isotopic composition almost identical with Emu Bay Shale.||||||
20045|Wilkawillina Limestone|67870|5|Briefly described|p9-10, p15, p21|Cambrian|Cambrian|Arrowie Basin. Appears on p9 as Wilawillina Formation. Source of bituminous hydrocarbons recovered from this unit.||Hawker Group.||Is overlain by Billy Creek Formation.||
20045|Wilkawillina Limestone|67907|6|Mentioned|p257, p259-260|||Flinders Ranges. Upper portion mentioned.||||||
20045|Wilkawillina Limestone|68030|5|Briefly described|p239|Cambrian|Cambrian|Flinders Ranges. Contains Ediacaran trilobites and archaeocyathids.||Unit of Hawker Group.||Overlain unconformably by, and channel infilled with Billy Creek Formation; laterally grades ino Mernmerna Formation. Underlain by Woodendinna Dolomite.||
20045|Wilkawillina Limestone|68735|5|Briefly described|p233, p234|Early Cambrian|Early Cambrian|See also mis-spelt Wilkawilina Limestone (p233 Fig.2). Arrowie Basin. The lower part of this formation has marked lateral facies changes.||Of the Hawker Group.||Underlain and intertongued by the Wirrapowie Limestone. Overlain by the Mernmerna Formation.|Lower: transgressive succession of lime mudstone, wackestone and isolated archeocyath-Renalcis bioherms. Middle: platform carbonates, many of which are biohermal.|10-APR-17
20045|Wilkawillina Limestone|69570|6|Mentioned|p420-p426, p428, p430, p432-p434|||Arrowie Syncline, Flinder Ranges. The upper part is interfingered with and partially overlain by the Wirrapowie Limestone. Fossil assemblage and sample localities are described.|||Includes the Hideaway Well Member, Woodendinna Dolostone, Winnitinny Creek Member and the Mount Mantell Member.|||
20045|Wilkawillina Limestone|70833|5|Briefly described|p176,178,180-188,190-201,203,205|Series 2|Terreneuvian|Of Arrowie Basin. Key sections: MORO and MOG (S of Moro Gorge, Arrowie Syncline); BALC (Balcoracana Gorge, Bunkers Range); MMT (Bunkers Range, central Flinders Ranges); WILK (Wilkawillina Type Section, Bunkers Graben); 10MS-W (Ten Mile South, SE Bunkers Graben).  Includes K. rostana and M. etheridgei zones in the lower and upper parts of the section respectively. Time-equivalent to uppermost Kulpara Limestone and lower half of Heatherdale Shale. Correlable to Ajz and Wirrapowie limestones.||Unit of Hawker Group.|Includes Second Plain Creek, Winnitinny Creek, Hideaway Well and Mount Mantell members.|Overlain by Mernmerna Formation. Underlain by Woodendinna Dolostone.||
20045|Wilkawillina Limestone|70835|5|Briefly described|p335-337, 351, 353|Cambrian|Cambrian|Arrowie Basin, Flinders Ranges. Type section is in Wilkawillina Gorge in the Bunkers Graben.||Hawker Group.|Mount Mantell, Hideaway Well, Winnitinny Creek, Members.|Overlies Woodendinna Dolostone. Is overlain unconformably by Mernmerna Formation.||
20045|Wilkawillina Limestone|71102|4|Described|p242,244-246,249,252,267,275|Series 2|Terreneuvian|Of Arrowie Basin. Intersected sections: DBS (Donkey Bore Syncline), MMF (Bunkers Range, Central Flinders Ranges), 10MS (10 Mile South, Bunkers Graben),  LMNB (Lower Mernmerna, North Boundary Creek, Chambers Gorge, E Flinders Ranges).|||Includes Winnitinny Creek Member.|Overlain by, and interfingers with Mernmerna Formation.|Bioclastic to clean micritic limestones. Rare muddy drapes.|
20045|Wilkawillina Limestone|72429|3|Fully described|p949, p952, p956, p959-961, p967|Lower Cambrian|Lower Cambrian|Mount Chambers Gorge, eastern Flinders Ranges. Up to 79m thick in measured section in the core of NE-SW-trending anticline. Outcrop is massive with beds up to 2m thick of silty yellow to buff-weathered partly dolomitic limestone with peloidal and oolitic interbeds of 0.5mm average grain diameter. It is internally pink to white with light grey patches and occasional limonitic buff-brown patches after weathered siderite. Stylolites and rare chert nodules are present. Fossils include abundant archaeocyaths, hyoliths and calciate brachiopods as well as large number tommotiid Micrina etheridgei, a zone fossil from the early Cambrian. Inferred habitat for the Wilkawillina Limestone fauna is biostromal mats or archaeocyath-calcimcirobe meadows scattered in the shallower and calmer waters of a shallow-marine shelf, but in the mid-platform away from high-energy margins. Clear-water sedimentation prevailed with well-agitated and oxygenated waters within the photic zone. Oolitic-to-peloidal shoals record active currents on the shelf. The environment corresponds to Shaw's least restricted zone of autochthonous sedimentary patterns in epeiric seas.||Hawker Group||Conformably underlies the Mernmerna Formation (Bendieuta Member). Interfingers with the Oraparinna Shale at top.|Massive, buff to pale yellow, silty to part sandy and oolitic archaeocyathan limestones, part dolomitic with calciate brachiopods.|
20045|Wilkawillina Limestone|72449|5|Briefly described|p1, p2 Map Legend|Cambrian|Cambrian|Shown in image on p1, 'Archaeocyaths in the Wilkawillina Limestone, Brachina Gorge' (photo 038766). Reefal limestone later formed a karst terrain.||||Overlies Bonney Limestone, ?Parachilna Formation, Woodendinna Dolomite and underlies Mernmerna Formation.|Light to dark grey, massive, bedded archaeocyathan limestone. A major erosional surface defined by karsting and a red weathering crust occurs within the unit.|
20045|Wilkawillina Limestone|73251|6|Mentioned|p36|Cambrian|Cambrian|Arrowie Basin, Moorowie and Yalkalpo Sub-basins. Thermally late to post-mature. Potential hydrocarbon reservoir and fairway.||Hawker Group||Unconformably overlain by Mernmerna Formation.||
20045|Wilkawillina Limestone|73255|6|Mentioned|p534 Fig.2|early Cambrian|early Cambrian|Contains Eoredlichia shensiensis trilobite fossils.||||Overlies the Woodendinna Dolomite, underlies the Bunkers Sandstone.|Carbonate rocks.|
20061|Willalooka Granite|42275|6|Mentioned|Table 2 p474|||geochemical analysis given.||||||24-AUG-18
20091|Willigan Member|22510|5|Briefly described|table1p37|||Age: Sturtian. Northern Flinders Ranges||||||
20091|Willigan Member|41405|6|Mentioned|p167|||||||||
20091|Willigan Member|67979|4|Described|p533-4, p529, p536 Fig.7|Marinoan||Locally occurring siltstone unit from Tindelpina area, formerly included in upper-most Tapley Hill Formation (Thomson et al. 1964), now considered in this article as a very localised, lower member of Yankaninna Formation. Thickness: 790 m. Overlies sedimentary mega-breccia unit, described (p533) as conformably overlying Tapley Hill Formation.||Yankaninna Formation|||Siltstones and shale.|22-SEP-14
20091|Willigan Member|71237|4|Described|p7, 10, 11, 19|||||||||
20109|Willouran Volcanics|24604|6|Mentioned|p915|||||||||
20109|Willouran Volcanics|37372|6|Mentioned|p3|||||||||
20109|Willouran Volcanics|41403|4|Described|p56|||||||||
20109|Willouran Volcanics|42222|6|Mentioned|p12|||||||||
20109|Willouran Volcanics|61153|6|Mentioned|p344-345 Fig. 1|||Of the Callanna Group. Geological Province: Adelaide Geosyncline.||||||
20135|Willyama Supergroup|6823|5|Briefly described|p203-205, 206, 233, 234, 236|Paleoproterozoic|Paleoproterozoic|Interpreted by Gustafson et al (1950) as a sequence of montonously alternating beds of clays, sandy clays and sands, intruded by thick granitic sills, thinner sills of gabbros and finally by sheets of pegmatite varying from very thick to very thin, all predominantly along bedding planes. This was more recently reinterpreted by Johnson and Klinger (1976), Stanton (1976), Archibald (1978), and Stevens et al (1983, 1988) as an upwards-fining, conformable 'layer cake' sequence 7-11km thick which can be correlated throught the Broken Hill Block. This sequence was supposedly punctuated by intervals of bimodal volcanism and minor exhalative chemical sediments. This study argues that the sequence includes granitic intrusions.|||||Garnet-cordeirite-sillimanite gneisses, amphibolites and augen and platy quartzo-feldspathic gneiss.|26-MAR-22
20135|Willyama Supergroup|22456|5|Briefly described|p16,fig15|||on map||||||
20135|Willyama Supergroup|22500|5|Briefly described|p 1||Proterozoic|Broken Hill Block||||||
20135|Willyama Supergroup|22553|3|Fully described|p75,fig1p76,p77||Proterozoic|||||||
20135|Willyama Supergroup|22575|4|Described|p178|Mesoproterozoic|Paleoproterozoic|||||||07-NOV-08
20135|Willyama Supergroup|22588|4|Described|p85|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
20135|Willyama Supergroup|22631|5|Briefly described|table1p171,fig2,p170|Statherian|Statherian|||||||
20135|Willyama Supergroup|22641|5|Briefly described|p687, Fig.2 p689|Paleoproterozoic|Paleoproterozoic|See also p693||||||07-NOV-08
20135|Willyama Supergroup|22671|5|Briefly described|p832,Fig1p835||Paleoproterozoic|Geological Province: Adelaide Fold Belt.||||||07-NOV-08
20135|Willyama Supergroup|22709|6|Mentioned|p201|||||||||
20135|Willyama Supergroup|22712|5|Briefly described|p131|Proterozoic|Proterozoic|||||||
20135|Willyama Supergroup|22720|6|Mentioned|Table 4 (p166)||Paleoproterozoic|Broken Hill Block||||||07-NOV-08
20135|Willyama Supergroup|22752|5|Briefly described|p 275||Paleoproterozoic|||||||07-NOV-08
20135|Willyama Supergroup|22771|4|Described|p44-45,Table12.2p45||Statherian|Max Age: 1720 Ma.||||||
20135|Willyama Supergroup|22772|6|Mentioned|p53,62,70||Paleoproterozoic|||||||07-NOV-08
20135|Willyama Supergroup|22773|5|Briefly described|Fig24.5p350|Precambrian|Precambrian|||||||
20135|Willyama Supergroup|22789|6|Mentioned|p50|||||||||
20135|Willyama Supergroup|22811|5|Briefly described|p604||Statherian|||||||
20135|Willyama Supergroup|22857|3|Fully described|p31, p44-45, p388 App1 Tb.A1.1|Paleoproterozoic|Paleoproterozoic|Multiply deformed metasedimentary schists and gneisses with abundant quartzofeldspathic gneisses, lesser mafic gneisses and minor 'lode' rocks. Max. Age: 1720Ma. Max. thickness: 9km. Geol.Prov: Adelaide Fold Belt (Willyama F.B.). See also p350 Fig.24.5.||||||07-SEP-09
20135|Willyama Supergroup|22858|6|Mentioned|p92,Fig14.9p100||Paleoproterozoic|||||||07-NOV-08
20135|Willyama Supergroup|22884|5|Briefly described|p40 Fig. 1, p39, p43 Fig3||Paleoproterozoic|Located across the Olary and Broken Hill Domains.||||||26-MAR-09
20135|Willyama Supergroup|22887|5|Briefly described|Fig.5 p12|Precambrian|Precambrian|||||||
20135|Willyama Supergroup|22933|6|Mentioned|Table11.1p5||Paleoproterozoic|||||||07-NOV-08
20135|Willyama Supergroup|22939|5|Briefly described|p243||Paleoproterozoic|||||||07-NOV-08
20135|Willyama Supergroup|22956|6|Mentioned|p146||Proterozoic|||||||
20135|Willyama Supergroup|22959|4|Described|p95,96,101||Paleoproterozoic|||||||07-NOV-08
20135|Willyama Supergroup|22960|4|Described|p89,90||Paleoproterozoic|||||||07-NOV-08
20135|Willyama Supergroup|22962|5|Briefly described|p73||Statherian|||||||
20135|Willyama Supergroup|22963|6|Mentioned|p67||Paleoproterozoic|||||||07-NOV-08
20135|Willyama Supergroup|22964|5|Briefly described|p53,54||Proterozoic|||||||
20135|Willyama Supergroup|22966|5|Briefly described|p2,4||Proterozoic|||||||
20135|Willyama Supergroup|22967|4|Described|p21,2,4-7,30,3,41,3,||Statherian|||||||
20135|Willyama Supergroup|23025|5|Briefly described|p74|Proterozoic|Proterozoic|||||||
20135|Willyama Supergroup|23068|5|Briefly described|p783|||||||||
20135|Willyama Supergroup|23093|5|Briefly described|p619||Paleoproterozoic|||||||07-NOV-08
20135|Willyama Supergroup|23094|5|Briefly described|p616|Proterozoic|Proterozoic|||||||
20135|Willyama Supergroup|23154|6|Mentioned|Map Legend|Mesoproterozoic|Mesoproterozoic|||||||
20135|Willyama Supergroup|23155|6|Mentioned|Fig 5 on p12|||||||||
20135|Willyama Supergroup|23160|5|Briefly described|p870 fig1||Proterozoic|||||||
20135|Willyama Supergroup|23210|5|Briefly described|p26||Paleoproterozoic|Curnamona Province.||||||07-NOV-08
20135|Willyama Supergroup|23223|5|Briefly described|p39, Fig.1|||Informally divided into upper (see p.40) and lower (see p.39) - Age: ~1720 - 1650 Ma. of Curnamona Province.||||||
20135|Willyama Supergroup|23248|5|Briefly described|p168||Paleoproterozoic|||||||07-NOV-08
20135|Willyama Supergroup|23336|6|Mentioned|p10|||||||||21-MAR-06
20135|Willyama Supergroup|23345|6|Mentioned|43|||||||||
20135|Willyama Supergroup|23346|5|Briefly described|48|||||||||
20135|Willyama Supergroup|23347|5|Briefly described|p51 Tb. 1, p53 Fig. 3|Statherian|Statherian|Age: ~1.71-1.64Ga. Comprises Strathearn and Curnamona Groups, Lady Louise and Basso Suites.||||||24-MAR-09
20135|Willyama Supergroup|23351|5|Briefly described|283|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
20135|Willyama Supergroup|23380|5|Briefly described|p105||Proterozoic|of Broken Hill Block. Age: Middle Proterozoic.||||||
20135|Willyama Supergroup|23391|6|Mentioned|p6|||||||||
20135|Willyama Supergroup|23476|5|Briefly described|p50|||||||||
20135|Willyama Supergroup|23477|5|Briefly described|p49 Fig 3|Mesoproterozoic|Paleoproterozoic|Geological Province: Curnamona Province.||||||07-NOV-08
20135|Willyama Supergroup|23478|5|Briefly described|p27|||Olary Province.||||||
20135|Willyama Supergroup|23565|5|Briefly described|p193|Paleoproterozoic|Paleoproterozoic|Geological Province: Broken Hill Block.||||||07-NOV-08
20135|Willyama Supergroup|23731|6|Mentioned|p15|||||||||
20135|Willyama Supergroup|23775|5|Briefly described|p721|||||||||22-SEP-09
20135|Willyama Supergroup|23801|6|Mentioned|p20|||||||||
20135|Willyama Supergroup|23912|5|Briefly described|p778|Proterozoic|Proterozoic|||||||
20135|Willyama Supergroup|24197|5|Briefly described|p62|||Dominates the Broken Hill Block region. Comprises 5 main groups including Thackaringa, Broken Hill, Sundown and Paragon Groups.||||||07-FEB-11
20135|Willyama Supergroup|24286|5|Briefly described|p25 Fig.2|||||||||
20135|Willyama Supergroup|24289|5|Briefly described|p42 Fig.1, p44, p46|Paleoproterozoic|Paleoproterozoic|Geological Province: Curnamona Province.||||||07-NOV-08
20135|Willyama Supergroup|24307|4|Described|p966|Proterozoic|Proterozoic|Thickness: 7000m.||||||21-OCT-08
20135|Willyama Supergroup|24431|5|Briefly described|p190|Statherian|Statherian|Age: ~1710 - 1650 Ma. Geological Province: Olary Domain.||||||
20135|Willyama Supergroup|24522|6|Mentioned|p80 Fig. 2|||Metasedimentary and bimodal meta-igneous rocks.  Age: 1.69Ga (Page and Laing 1992). Geological Province: Curnamona Province (SA).  See also p82.||||||
20135|Willyama Supergroup|24526|5|Briefly described|p99|Paleoproterozoic|Paleoproterozoic|Metasedimentary rocks.  Age: c.1710-1649Ma.  Geological Province: Curnamona Craton.||||||07-NOV-08
20135|Willyama Supergroup|24582|5|Briefly described|p4|Paleoproterozoic|Paleoproterozoic|Includes Wiperaminga Subgroup. In the Olary Block.  Geological Province: Curnamona Province.||||||07-NOV-08
20135|Willyama Supergroup|24592|4|Described|p634|Paleoproterozoic|Paleoproterozoic|Age: ca. 1710 - 1640 Ma. Of the Willyama Supergroup. Geological Province: Curnamona Province. Divided into the basal Quartzo-feldspathic Suite, and overlying Calc-silicate and Pelite Suites based on magnetic susceptibility.||||||09-MAY-13
20135|Willyama Supergroup|38969|4|Described|p199|||||||||
20135|Willyama Supergroup|39662|2|Defined|p408|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
20135|Willyama Supergroup|39849|6|Mentioned|p86|||See also P87||||||
20135|Willyama Supergroup|39883|6|Mentioned|p380|||||||||
20135|Willyama Supergroup|39885|6|Mentioned|p427|||||||||
20135|Willyama Supergroup|40290|6|Mentioned|p1|||||||||
20135|Willyama Supergroup|40291|6|Mentioned|p9|||See also Fig.3||||||
20135|Willyama Supergroup|40448|5|Briefly described|p30|||||||||
20135|Willyama Supergroup|40582|6|Mentioned|p467|||||||||
20135|Willyama Supergroup|40595|5|Briefly described|p73|||||||||
20135|Willyama Supergroup|40642|6|Mentioned|p163|||||||||
20135|Willyama Supergroup|40914|6|Mentioned|Map legend|Mesoproterozoic|Paleoproterozoic|Early to Middle Proterozoic||||||07-NOV-08
20135|Willyama Supergroup|41006|6|Mentioned|p292|||||||||
20135|Willyama Supergroup|41092|6|Mentioned|Table 1|||||||||
20135|Willyama Supergroup|41093|4|Described|p250|||||||||
20135|Willyama Supergroup|41145|3|Fully described|p827|||||||||
20135|Willyama Supergroup|41402|5|Briefly described|p37|||||||||
20135|Willyama Supergroup|41403|6|Mentioned|p48|||||||||
20135|Willyama Supergroup|41419|6|Mentioned|p379|||||||||
20135|Willyama Supergroup|41526|6|Mentioned|p14|||||||||
20135|Willyama Supergroup|41630|5|Briefly described|p3|||||||||
20135|Willyama Supergroup|41633|6|Mentioned|p154|||See also Fig.2.27||||||
20135|Willyama Supergroup|41651|6|Mentioned|p188|||||||||
20135|Willyama Supergroup|41652|5|Briefly described|p193|||||||||
20135|Willyama Supergroup|41791|5|Briefly described|p267|||||||||
20135|Willyama Supergroup|41859|6|Mentioned|p426|||||||||
20135|Willyama Supergroup|41870|6|Mentioned|p131|||||||||
20135|Willyama Supergroup|41978|6|Mentioned|p495|||||||||
20135|Willyama Supergroup|42090|3|Fully described|p14|||See also Table 2||||||
20135|Willyama Supergroup|42098|6|Mentioned|p57|||||||||
20135|Willyama Supergroup|42171|6|Mentioned|p142|||||||||
20135|Willyama Supergroup|42181|6|Mentioned|p252|||||||||
20135|Willyama Supergroup|42223|6|Mentioned|Fig.2 P36|||||||||
20135|Willyama Supergroup|42261|6|Mentioned|p529|||See also Fig.1 P530.||||||
20135|Willyama Supergroup|42263|6|Mentioned|p15|||With "quartz bands up to 1/2" thick are drag and reverse folded".||||||
20135|Willyama Supergroup|42286|6|Mentioned|p7|||||||||
20135|Willyama Supergroup|42323|5|Briefly described|p3|Mesoproterozoic|Paleoproterozoic|||||||07-NOV-08
20135|Willyama Supergroup|42357|6|Mentioned|p8|||||||||
20135|Willyama Supergroup|42507|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
20135|Willyama Supergroup|42527|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
20135|Willyama Supergroup|42528|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
20135|Willyama Supergroup|42529|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
20135|Willyama Supergroup|42530|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
20135|Willyama Supergroup|42531|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
20135|Willyama Supergroup|42537|5|Briefly described|p3|||||||||
20135|Willyama Supergroup|42595|5|Briefly described|p3, p5|||||||||
20135|Willyama Supergroup|42672|5|Briefly described|p372|||||||||
20135|Willyama Supergroup|42720|5|Briefly described|map legend|Paleoproterozoic||||||||07-NOV-08
20135|Willyama Supergroup|42725|5|Briefly described|p5|||||||||
20135|Willyama Supergroup|42746|6|Mentioned|p3|||||||||
20135|Willyama Supergroup|42755|6|Mentioned|p4|||||||||
20135|Willyama Supergroup|42813|4|Described|p9|||||||||
20135|Willyama Supergroup|42819|5|Briefly described|p315|||||||||
20135|Willyama Supergroup|42871|5|Briefly described|p88|||||||||
20135|Willyama Supergroup|42897|5|Briefly described|p319|||see also Fig.3, P321||||||
20135|Willyama Supergroup|42942|6|Mentioned|p17|||||||||
20135|Willyama Supergroup|42966|5|Briefly described|Fig.25 p47|||||||||
20135|Willyama Supergroup|42982|5|Briefly described|Fig.1,p332|||||||||
20135|Willyama Supergroup|42991|6|Mentioned|Fig.3|||||||||
20135|Willyama Supergroup|43052|4|Described|p82|||||||||
20135|Willyama Supergroup|43086|5|Briefly described|p1|||||||||
20135|Willyama Supergroup|43141|6|Mentioned|p63,Fig.1|||||||||
20135|Willyama Supergroup|43192|6|Mentioned|p62|||Same as Willyama Complex,p58.||||||
20135|Willyama Supergroup|43213|6|Mentioned|p63|Mesoproterozoic|Mesoproterozoic|Broken Hill Block. Tentatively equated with Ponto beds of Wonominta Block.||||||
20135|Willyama Supergroup|43264|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
20135|Willyama Supergroup|43265|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
20135|Willyama Supergroup|43266|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
20135|Willyama Supergroup|43267|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
20135|Willyama Supergroup|43268|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
20135|Willyama Supergroup|43269|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
20135|Willyama Supergroup|43270|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
20135|Willyama Supergroup|43271|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
20135|Willyama Supergroup|43272|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
20135|Willyama Supergroup|43273|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
20135|Willyama Supergroup|43274|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
20135|Willyama Supergroup|43485|5|Briefly described|2-3|||||||||
20135|Willyama Supergroup|43561|5|Briefly described|Fig.3,1434,1438|||1690 Ma||||||
20135|Willyama Supergroup|43572|6|Mentioned|p5||Paleoproterozoic|||||||07-NOV-08
20135|Willyama Supergroup|43583|6|Mentioned|p2138|||||||||
20135|Willyama Supergroup|43591|6|Mentioned|p163|||||||||
20135|Willyama Supergroup|43595|4|Described|p75,354-5|||Max. age of deposition: approx. 1.82 Ga, high-grade metamorphism: 1.66 Ga, intruded at 1.49 Ga||||||
20135|Willyama Supergroup|43685|5|Briefly described|p243||Paleoproterozoic|||||||07-NOV-08
20135|Willyama Supergroup|44093|5|Briefly described|p28, p41|Mesoproterozoic|Paleoproterozoic|See also p139 Appendix 1. Supersedes the Willyama "Complex". Sequence of highly deformed metasedimentary and meta-igneous schists and gneisses, and minor 'lode' rocks. Forms the Australian Craton. Geological Province: Willyama Fold Belt.||||||09-JUL-13
20135|Willyama Supergroup|44195|6|Mentioned|p349|||Broken Hill. Compared to Soldiers Cap Group.||||||
20135|Willyama Supergroup|46598|3|Fully described|p298|||||||||
20135|Willyama Supergroup|50045|5|Briefly described|p116, p116 Fig. 3|||Geological Province: Broken Hill Block. Includes the Thackaringa Group, Broken Hill Group and Paragon Group.||||||31-MAY-07
20135|Willyama Supergroup|50081|5|Briefly described|p43|Statherian|Statherian|Age: ~1710-1640 Ma. Geological Province: Curnamona Province.||||||24-FEB-05
20135|Willyama Supergroup|50547|5|Briefly described|p1226|||||||||
20135|Willyama Supergroup|50605|6|Mentioned|p6.1, 9.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Olary Block. Intruded by Olary 1590 Ma Supersuite.||||||07-NOV-08
20135|Willyama Supergroup|50606|6|Mentioned|p1.1|||Geological Province: Broken Hill Block.||||||
20135|Willyama Supergroup|50619|5|Briefly described|p174 Fig. 1, p178 Fig. 3|Paleoproterozoic|Paleoproterozoic|Comprises the Paragon, Sundown, Broken Hill and Thackaringa Groups, Thorndale Composite Gneiss and the Clevedale Migmatite.  Geological Province: Broken Hill Block.  See also p175.||||||07-NOV-08
20135|Willyama Supergroup|60485|5|Briefly described|p28 Fig. 2|||Geological Province: Olary and Broken Hill Domains.||||||
20135|Willyama Supergroup|60953|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Age: ~1730-1650Ma. Greenschist to granulite facies metasediments and mafic and felsic metavolcanics and intrusives.||||||07-NOV-08
20135|Willyama Supergroup|60959|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Undifferentiated metasediments.||||||07-NOV-08
20135|Willyama Supergroup|61032|5|Briefly described|p6|Paleoproterozoic|Paleoproterozoic|Includes Wiperaminga Subgroup.||||||07-NOV-08
20135|Willyama Supergroup|61108|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|Metasediment and felsic metavolcanic rock, greenschist to granulite facies. Mafic and felsic metamorphosed volcanic and intrusive rock. Age: ~1730-1650 Ma.||||||07-NOV-08
20135|Willyama Supergroup|61235|5|Briefly described|p13 Fig. 1|||Geological Province: Curnamona Province.||||||11-AUG-05
20135|Willyama Supergroup|61239|5|Briefly described|p53 Fig. 1|||||||||
20135|Willyama Supergroup|61262|5|Briefly described|p455 Fig. 11|Paleoproterozoic|Paleoproterozoic|Geological Province: Broken Hill.||||||07-NOV-08
20135|Willyama Supergroup|61311|6|Mentioned|p42|||||||||
20135|Willyama Supergroup|61314|6|Mentioned|p120|||||||||
20135|Willyama Supergroup|61318|5|Briefly described|p580.|Proterozoic|Proterozoic|Hosts a major stratiform Zn-Pb-Ag ore deposit at Broken Hill. General north-to-south increase of metamorphic grade from greenschist to granulite facies. Rocks have been folded and sheared.|||||Metamorphosed sequence of pelitic to psammitic sediments, subordinate felsic and mafic volcanic rocks and minor intercalated intrusive rocks.|
20135|Willyama Supergroup|61605|5|Briefly described|p768, p769|Paleoproterozoic|Paleoproterozoic|Incl: Thackaringa and Broken Hill Gps. Aluminous metasedimentary gneisses+locally abundant albite-rich rocks, basic gneisses (amphibolites), lesser quartzo-feldspathic gneisses; substantial bodies of deformed pegmatite and leucocratic quartzo-feldspathics||||||07-NOV-08
20135|Willyama Supergroup|61734|5|Briefly described|p51, p52 Fig.2, p54, p56, p67-68|Mesoproterozoic|Paleoproterozoic|Deposition in intracontinental rift or continental back-arc basin.|1720-1640 Ma||Includes the Curnamona and Strathearn Groups.||Package of metasedimentary and metavolcanic rocks.|
20135|Willyama Supergroup|61735|5|Briefly described|p634, p635 Fig. 1|Paleoproterozoic|Paleoproterozoic|Geological province: Broken Hill Domain. Discussed from a geochronological aspect. See also p636 Fig. 2.||||||04-JUN-15
20135|Willyama Supergroup|61736|4|Described|p663|Paleoproterozoic|Paleoproterozoic|Subdivided into Lower and Upper Willyama Supergroups. Geological province: Broken Hill Domain. Chronostratigraphy discussed on p670-71.||||||24-FEB-10
20135|Willyama Supergroup|61822|5|Briefly described|p104|Paleoproterozoic|Paleoproterozoic|Part of the southern Broken Hill Domain and the southeastern Euriowie Domain.||||||07-NOV-08
20135|Willyama Supergroup|61825|5|Briefly described|p130|Paleoproterozoic|Paleoproterozoic|Metasediments and meta-igneous rocks. Intruded by Mundi Mundi Granites. Geological Province: Broken Hill Domain and Eurowie Domain.||||||07-NOV-08
20135|Willyama Supergroup|61908|5|Briefly described|p146|Paleoproterozoic|Paleoproterozoic|Geological Province: Broken Hill Block.||||||07-NOV-08
20135|Willyama Supergroup|61936|6|Mentioned|p203|||Geological Province: Curnamona Province.||||||
20135|Willyama Supergroup|62373|5|Briefly described|p502|Paleoproterozoic|Paleoproterozoic|Metasedimentary sequence. Age: 1715-1645 Ma (Page et al 1998, 2000, 2003). Geological Province: Curnamona Province - Olary and Broken Hill Domains.||||||09-JUL-13
20135|Willyama Supergroup|62473|5|Briefly described|p72-74|||Stratigraphic coherence of the rocks of this supergroup is debated.||||||17-JUN-09
20135|Willyama Supergroup|62514|5|Briefly described|p746|||Basso Suite included. Includes pelitic and psammitic metasediments. Geological Province: Olary Domain/Curnamona Province.||||||09-JUL-13
20135|Willyama Supergroup|62535|5|Briefly described|p663-665, p668, p670-674|Paleoproterozoic|Paleoproterozoic|Dominant unit in the Curnamona Province. Base and top are indeterminate; thickness estimated at c.7 km. Multiply deformed, metamorphosed and locally intensely metasomatically altered during the ~1600 Ma Olarian Orogeny. Hosts minor strata-bound gold mineralization. Correlations discussed.|~1720-1640 Ma.||Broken Hill Group.|||
20135|Willyama Supergroup|62536|5|Briefly described|p633-636, 638, 640, 642, 647, 649, 651|Paleoproterozoic|Paleoproterozoic|See also p653, 655, 657-659. Broken Hill area. Deposition spanned ~70 m.y.|||Thackaringa, Broken Hill Groups.||Metasedimentary and metavolcanic rocks.|
20135|Willyama Supergroup|62592|4|Described|pp12-15, p16 Fig.2.2, p43, pp73-76, p78.|Late Paleoproterozoic|Late Paleoproterozoic|Curnamona Province. About 20,000 km2 in area and >7 km thick; neither top nor base have been observed. A-type plutons aged c.1712 Ma intrude the earliest rocks of this unit. Youngest bimodal magmatism was c.1685 Ma; youngest preserved sedimentary rocks are c.1640 Ma, with a further 20 m.y. deposition equivalent to the upper McNamara Group of the Mount Isa Inlier.|c.1718 - <1640 Ma.||Includes Thackaringa, Broken Hill, Sundown, Paragon, Curnamona and Strathearn Groups.||Bimodal volcanics and shallow-water sedimentary deposits, with deeper-water deposition in upper parts.|
20135|Willyama Supergroup|62641|6|Mentioned|p275, p286, p288-289.|||Curnamona (Broken Hill) region. Provenance correlations drawn with Nawa Domain (South Australian Craton) and Maronan Supergroup (Mount Isa region) suggest contiguity during late Paleoproterozoic; the lower part  of the Supergroup received detritus from Arunta region. It contains syn-depositional intrusives aged c.1715 Ma.||||||
20135|Willyama Supergroup|62724|5|Briefly described|p17 Fig. 4|Mesoproterozoic|Paleoproterozoic|First called "Willyama Complex" (Mawson 1912). Geological Province: Broken Hill and Olary Domains / Curnamona Province. See also p16 Fig. 2.||||||07-FEB-11
20135|Willyama Supergroup|62727|5|Briefly described|p8|||Host to uranium by cavity fill (fractures, veins, apophyses - within sodic granitoids of the group).  Geological Province: Curnamona Province.||||||
20135|Willyama Supergroup|62728|5|Briefly described|p26, p28|||Conformably encloses gneisses of the Basso Suite. See also Willyama Supergroup metasediments.||||||07-FEB-11
20135|Willyama Supergroup|62993|5|Briefly described|p1-6, 12,14-16,18,20, 22,23,28-32,35, 37|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain and Olary Domains. See also figs on pp40, 44.|||Includes Broken Hill Group, Curnamona Group, Strathearn Group, Thackaringa Group, Rantyga Group, Sundown Group, Paragon Group|Intruded by Basso Suite, Bimbowrie Suite|Psammopelitic, psammitic, calcareous and calc-albititc metasediments.Pelitic kyanite bearing metasediments,|19-DEC-21
20135|Willyama Supergroup|63020|6|Mentioned|p971|||||||||
20135|Willyama Supergroup|63056|5|Briefly described|p81 Fig. 2|Proterozoic|Proterozoic|||||||
20135|Willyama Supergroup|63102|5|Briefly described|p7-8,10, 12-14,22,32,35-36,38-39,44,52|Mesoproterozoic|Paleoproterozoic|Geological province: Curnamona Province. Total thickness unknown as neither top nor base have been observed. Estimated to be approximate 5km in Olary Domain (Laing 1996b), but between 4.5-13km in the Broken Hill Domain (Willis et al 1983). Source material for the Willyama Supergroup that is older than Mount Howden and Paragon groups may be the Arunta terrane of central Australia. See also p47, p60-61,63,67.|||Includes Broken Hill and Curnamona groups.|||22-OCT-19
20135|Willyama Supergroup|63110|6|Mentioned|p1130|||||||||
20135|Willyama Supergroup|63186|4|Described|p66|Paleoproterozoic|Paleoproterozoic|Includes Thackaringa Group, and Wiperaminga and Ethiudna Subgroups. Age: 1720-1645 Ma. Geological Province: Curnamona Province.||||||07-NOV-08
20135|Willyama Supergroup|63489|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Represented by unnamed and undifferentiated metsediments and units. Geological Province: Mount Painter Inlier and Mount Babbage Inlier.||||||07-NOV-08
20135|Willyama Supergroup|63519|5|Briefly described|p8, p10 Fig. 3|Paleoproterozoic|Paleoproterozoic|Geological Province: Broken Hill Block-Euriowie Block.||||||07-NOV-08
20135|Willyama Supergroup|63539|5|Briefly described|p33 Fig. 1a|||Geological Province: Curnamona Province.||||||07-FEB-08
20135|Willyama Supergroup|63793|6|Mentioned|pp10-11.|||Broken Hill Block.||||||
20135|Willyama Supergroup|63866|4|Described|p34-p42, p44, p48|Statherian|Statherian|Broken Hill and Olary Domains, Curnamona Province. Deposited in a shallow marine environment. Rocks are metamorphosed to granulite-facies in the south and greenschist facies to the north. Informally subdivided into an upper and lower part on p38. Appears as the Willyama SG on p37. Also includes the Clevedale Migmatite, Thorndale Composite Gneiss, Redan Gneiss, Ednas Gneiss, Mulculca Formation|1719-1640 Ma||Includes the Broken Hill Group and the Thackaringa Group, Sundown Group, Curnamona Group, Paragon Group and the Strathearn Group.||Psammites, pelites, calc-silicates and carbonates. The lower part consists of migmatites, metasedimentary rocks, psammitic to psammopelitic gneisses passing up into gneisses interpreted as metamorphosed rhyodacitic flows or tuffs.|
20135|Willyama Supergroup|64097|4|Described|p302|Paleoproterozoic|Paleoproterozoic|Includes Thackaringa, Broken Hill and Paragon Gps, and new Rantyga Group. Geol Prov: Broken Hill Domain + Olary Domain/Curnamona Prov.Succession of metaseds.+ minor metavolcs., extensively intruded ??..Considerable age evidence for constituents discussed.||||||07-FEB-11
20135|Willyama Supergroup|64130|6|Mentioned|p1382 |||Curnamona Province. Hosts the giant Broken Hill Pb-Zn-Ag deposit.||||||
20135|Willyama Supergroup|64249|6|Mentioned|p102|||Geological Province: Eastern Fold Belt. Albites are abundant in this unit.||||||22-APR-09
20135|Willyama Supergroup|64250|6|Mentioned|p25 fig 10|||Broken Hill Province.|||Includes Thackaringa, Broken Hill, Sundown, Paragon Groups.|||
20135|Willyama Supergroup|64316|5|Briefly described|p532, p533 Fig. 1|Paleoproterozoic|Paleoproterozoic|Includes Thackaringa, Broken Hill, Sundown and Paragon Groups. Upper section is turbiditic metasedimentary package dominated by Sundown Group. Geological Province: Broken Hill Block.||||||07-FEB-11
20135|Willyama Supergroup|64576|6|Mentioned|p636|||||||||
20135|Willyama Supergroup|64722|5|Briefly described|Fig. 2 p3-6, p14-15, 22|Statherian|Statherian|Curnamona Province. Age from intercalated tuffs.|1720 - 1640 Ma.||Contains Weekaroo Amphibolite; Bumba Formation (Olary Block); Paragon, Sundown, Broken Hill, Thackaringa Groups; Thorndale Gneiss; Clevedale Migmatite (Broken Hill region).|||11-APR-12
20135|Willyama Supergroup|64724|5|Briefly described|p46|Proterozoic||||||||
20135|Willyama Supergroup|64725|5|Briefly described|p58 Fig.2, pp71-72.|||Olary-Willyama Block. Sedimentary and bimodal volcanic rocks; hosts the stratiform Broken Hill massive sulfide deposits.|c.1730-1700 Ma.|||||
20135|Willyama Supergroup|64726|6|Mentioned|p89.|||Deeper water sedimentation along the eastern margin of the Australian continent after c.1670 Ma.||||||
20135|Willyama Supergroup|64741|4|Described|p297-8, p312-313|Paleoproterozoic|Paleoproterozoic|Age: ~1720-1640Ma. Geological province: Broken Hill and Olary Domains, Curnamona Province.||||||07-FEB-11
20135|Willyama Supergroup|64742|4|Described|pp318-335.|Paleoproterozoic|Paleoproterozoic|Curnamona Province. Metamorphosed to granulite facies during the c.1600 Ma Olarian Orogeny; later (c.500 Ma) by the Delamerian Orogeny. Contains the world's largest known Pb-Zn-Ag deposit at Broken Hill. c.7 km thick.|||Includes Curnamona and Strathearn Groups in the Olary Domain; and Thackaringa, Broken Hill, Sundown and Paragon Groups in the Broken Hill Domain.||Sequence of generally shallow water metamorphosed quartzofeldspathic and pelitic sedimentary rocks, calc-silicates, minor volcanic and subvolcanic rocks.|
20135|Willyama Supergroup|64743|5|Briefly described|pp339-343, p346 Fig.7.|Paleoproterozoic|Paleoproterozoic|Discusses timing and tectonism of deformation of this unit.|||Includes Thackaringa, Broken Hill, Sundown and Paragon Groups.|||
20135|Willyama Supergroup|64744|5|Briefly described|pp352-354, p356, pp359-360, pp362-367.|Statherian|Statherian|Includes rocks from Calvert and Isa superbasins. Deformed and metamorphosed up to granulite facies. Intruded by S- and A-type granites, and mafic dykes and sills, between 1710-1680 Ma.|||SA = Wiperaminga, Ethiudna, Saltbush and Mount Howden Subgroups. NSW = Redan, Thorndale Composite, Alma, Rasp Ridge Gneisses; Clevedale Migmatite; Thackaringa, Broken Hill, Sundown, Paragon Groups.|||
20135|Willyama Supergroup|64896|6|Mentioned|p1390|||Geological Province: Curnamona Province.||||||
20135|Willyama Supergroup|64944|6|Mentioned|p26, p28 Fig. 1|Paleoproterozoic|Paleoproterozoic|Geological province: Olary Domain.||||||07-FEB-11
20135|Willyama Supergroup|65194|6|Mentioned|p40, p42-43|||||||||
20135|Willyama Supergroup|65220|5|Briefly described|p20, p21 Fig. 3|Paleoproterozoic|Paleoproterozoic|of the Curnamona Province. Informal subdivisions and age: 1715-1600 Ma shown in Fig. 3||||||10-DEC-09
20135|Willyama Supergroup|65375|6|Mentioned|p13.|Paleoproterozoic|Paleoproterozoic||c.1720-1640 Ma.|||||
20135|Willyama Supergroup|65376|6|Mentioned|p9 Fig.1.2. |Paleoproterozoic|Paleoproterozoic||||||Metasediments and felsic volcanic rocks.|
20135|Willyama Supergroup|65390|6|Mentioned|p27 Fig. 6|Statherian|Statherian|Curnamoma Province. Age c.1720 - 1640 Ma.||||||
20135|Willyama Supergroup|65407|5|Briefly described|p238|Paleoproterozoic|Paleoproterozoic|Basement to Curnamona Province.|||||Metasedimentary and metavolcanic rocks.|
20135|Willyama Supergroup|65489|6|Mentioned|p18, p120|Proterozoic|Proterozoic|Part of basement to Warburton Basin.||||||
20135|Willyama Supergroup|65681|6|Mentioned|pp733-734,|Paleoproterozoic|Paleoproterozoic||c.1690 Ma.||Includes Feral gneiss, Alma and Rasp Ridge Gneisses.|||16-MAY-13
20135|Willyama Supergroup|65756|5|Briefly described|p27, 38|Mesoproterozoic|Paleoproterozoic|||||||
20135|Willyama Supergroup|65925|5|Briefly described|p61, p64, p79, Appendix 2.|Paleoproterozoic|Paleoproterozoic|Curnamona Province. Metasedimentary and metaigneous rocks. Several granitoid suites have high uranium contents.|||||Composite gneiss suite; calc-silicate suite; amphibolite; quartzofeldspathic gneiss.|
20135|Willyama Supergroup|66302|4|Described|p7-p9, p35-p38, p40-41, p48-p52, p64|Statherian|Statherian|Broken Hill Domain, Olary Domain, Curnamona Province. Estimated to be between 7 and 13km thick. Age derived from Nutman and Gibson (1998) and Page et al. (2000). See also p72-73, p75-77, p80-81, p88-89.|ca. 1710 to 1600 Ma||Includes the Curnamona Group, Broken Hill Group, Thackaringa Group, Paragon Group, Rantyga Group, Strathearn Group, Portia Formation and the Sundown Group.|Unconformably overlain by the Benagerie Volcanics. Intruded by the Silver City Suite. Probably equivalent to the Barossa Complex.|Metasedimentary and metavolcanic rocks.|
20135|Willyama Supergroup|66518|6|Mentioned|p18, p19 Fig.4, p22.|Paleoproterozoic|Paleoproterozoic|Forms part of the basement of the Curnamona Province.||||||
20135|Willyama Supergroup|66522|6|Mentioned|p28.|Proterozoic|Proterozoic|Likely source of detrital zircons found in Kooringa Member.||||||
20135|Willyama Supergroup|66800|6|Mentioned|p933.|||Central part has been correlated (Laing & Beardsmore 1986) with older part of Etheridge Group. Also, Laing (1996b) calculated a sedimentation rate for the central part of this unit at 1 mm/yr.||||||
20135|Willyama Supergroup|66857|5|Briefly described|p971, p976.|Paleoproterozoic|Paleoproterozoic|Broken Hill and Olary Domains. Metamorphosed during Mesoproterozoic Olarian Orogeny. Relict fragmental and porphyritic textures are preserved in quartzo-feldspathic gneisses, originally rhyolitic volcaniclastics and co-magmatic A-type granitoids.|||||Pelitic, psammopelitic and psammitic schists and gneisses, albitic and calc-silicate rocks, banded iron-formation and garnet-quartz rocks.|
20135|Willyama Supergroup|67058|5|Briefly described|p494 Fig.14, p497.|||Curnamona Province. Shows detrital zircon probability plots with peaks at 1685, 1790, 2660 and 2980 Ma. The upper part of the Supergroup is aged 1655-1640 Ma.||||||
20135|Willyama Supergroup|67181|5|Briefly described|p632 Fig.14, p633 Fig.15, |Statherian|Statherian|Curnamona Province, metasediments. Age from Fig.14 Barovich and Hand (2008).|c.1710-1670 Ma|||||
20135|Willyama Supergroup|67323|5|Briefly described|p33 Fig.4.6, p34-35|Paleoproterozoic|Paleoproterozoic|Curnamona Province. Intraplate magmatism. Underwent a depositional hiatus ~1680-1670 Ma, and partial melting ~1640 Ma.||||||
20135|Willyama Supergroup|67536|5|Briefly described|Map Legend|||Curnamona Province.|||Includes Strathearn, Broken Hill and Curnamona Groups.|Possible equivalent of the Radium Creek Metamorphics ?|Metasediments.|
20135|Willyama Supergroup|67540|5|Briefly described|p25, p26 Fig.1, p29,31 Tb.2, p37|||The intrusions (granites and minor alkaline and mafic rocks) and volcanics in central Curnamona Province are now called the Ninnerie Supersuite and they variously intrude and overlie the Willyama Supergroup.|||Includes Tommie Wattie Formation, Ameroo Subsuite, Ethiudna Subgroup.|Intruded by the Crocker Well Suite and Bimbowrie Suite. Overlain by the Benagerie Volcanic Suite.||04-FEB-16
20135|Willyama Supergroup|67581|6|Mentioned|p44 Fig.8, 45|||Curnamona Province. Intrusive and extrusive magmatic activity occurred synchronously with deposition of sediments in the lower part of this Supergroup.|||Basso, Silver City and Lady Louise Suites; Redan, Farmcote and Hores Gneisses.|||
20135|Willyama Supergroup|67653|5|Briefly described|p3-4|Late Paleoproterozoic|Late Paleoproterozoic|Geological province: Curnamona Province.|||Includes Stratheam, Broken Hill and Curnamona groups.|||
20135|Willyama Supergroup|67900|5|Briefly described|p18-19|Paleoproterozoic|Paleoproterozoic|Curnamona Province. Underwent polyphase deformation and metamorphism during the Olarian and Delamerian Orogenies.|1720-1640 Ma.|||Is intruded by Ninnerie Supersuite.|Metasedimentary and meta-igneous rocks.|
20135|Willyama Supergroup|68021|6|Mentioned|p131|Statherian|Statherian|Shown as lower Willyama Supergroup, Age 1730-1670 Ma.||||||
20135|Willyama Supergroup|68068|5|Briefly described|Map legend|||Curnamona Province.||||||
20135|Willyama Supergroup|68126|4|Described|p1-2, p6, p26, p30-31, p33, p48|Paleoproterozoic|Paleoproterozoic|Curnamona Province. Geochronology data for constituent units listed. Metamorphism at 1602 +/- 4 Ma. Geochemical analyses detailed. Appears as Willyama Supersuite on p48.|<1796 +/- 10 Ma (maximum depositional age).||Strathearn, Curnamona, Paragon, Sundown, Broken Hill, Thackeringa Groups; Thorndale Composite Gneiss.||Metasediments, quartzofeldspathic gneiss, composite gneiss, quartz-albite rocks, basic gneiss, calc-silicate and calc-albitite rocks; and metavolcanics.|
20135|Willyama Supergroup|68131|5|Briefly described|p2 Fig.1|Paleoproterozoic|Paleoproterozoic||||||Metasediments and felsic volcanic rocks.|
20135|Willyama Supergroup|68158|6|Mentioned|p17|||Curnamona Province.|~1715 Ma -~1650 Ma.|||||
20135|Willyama Supergroup|68315|6|Mentioned|p764-766, 771-772|Paleoproterozoic|Paleoproterozoic|Curnamona Province. Underwent LP-HT amphibolite- to granulite-grade metamorphism in the c.1610-1590 Ma Olarian Orogeny.||||||
20135|Willyama Supergroup|68731|6|Mentioned|p170 Fig 3.83|Proterozoic|Proterozoic|||||||
20135|Willyama Supergroup|69023|5|Briefly described|p13 Fig.4, p15, p72-73, p79-80, p145|Proterozoic|Proterozoic|Geochronology suggests there may be no rocks of this unit in Mount Painter Province. Equated with Radium Creek Metamorphics on stratigraphic, but not radiometric, grounds.||||||
20135|Willyama Supergroup|69213|5|Briefly described|p32-35|Paleoproterozoic|Paleoproterozoic||1720-1640 Ma||Includes Curnamona Group||Metasediments with lesser volcanic components. Migmatites range from stromatic migmatites to diatexite migmatite . Stromatic migmatite is intruded by foliated, syntectonic leucogranite sheets.|
20135|Willyama Supergroup|69255|6|Mentioned|p788|Paleoproterozoic|Paleoproterozoic||||||Metasedimentary rocks.|
20135|Willyama Supergroup|69562|6|Mentioned|p665, p674 Fig.6|||||||||
20135|Willyama Supergroup|69567|6|Mentioned|p277|||Broken Hill.|||||Includes tourmalinites (tourmaline metaquartzites).|
20135|Willyama Supergroup|69591|6|Mentioned|p107 Fig.2.102|||Appears in a diagram of the geodynamic setting of ~1725-1690 Ma eastern Australia.||||||
20135|Willyama Supergroup|69650|4|Described|p1, p2, p5-6, p15-16, p21-23, p27-29|Paleoproterozoic|Paleoproterozoic|See also p34-35, p38, p41, p45. Southern Curnamona Province. Probable crustal source of most of Ninnerie Supersuite. Appears as Upper and Lower Willyama Supergroup on p16,29,34,38,41,45.|1720-1640 Ma.||Includes Ethiudna Subgroup, Tommie Wattie Formation, Bimba and Peryhumuck Formations.|Intruded and overlain by Ninnerie Supersuite.||
20135|Willyama Supergroup|69654|6|Mentioned|p2, 6, 25|Paleoproterozoic|Paleoproterozoic|Southern Curnamona Province.||||||
20135|Willyama Supergroup|69982|5|Briefly described|p15, p17-19, p45, p69, p86, p220|Paleoproterozoic|Paleoproterozoic|Forms crystalline basement below the southern Cooper Basin. Brief thin section descriptions. Bedding dip angles in wells listed.|||||Includes schists and phyllite.|
20135|Willyama Supergroup|69999|5|Briefly described|p1, p4, p17, p21|Paleoproterozoic|Paleoproterozoic|Willis et al. (1983). Broken Hill and Euriowie Blocks. Preserves evidence of two major metamorphic events: a prograde field gradient at c.1600 Ma (Olarian Orogeny) and a retrograde field gradient at c.500 Ma (Delamerian Orogeny).|||||A metamorphosed sequence of pelitic to psammitic sedimentary rocks with intercalated mafic/felsic volcanic and plutonic rocks.|
20135|Willyama Supergroup|70000|5|Briefly described|p31, p33-34|Statherian|Statherian||||Includes Curnamona, Rantyga, Thackaringa, Broken Hill, Sundown and Paragon Groups.|||
20135|Willyama Supergroup|70014|5|Briefly described|Map legend||||||Includes Redan, Ednas, and Thorndale Composite, Gneisses; Clevedale Migmatite; Mulculca Formation; Thackaringa, Broken Hill, Sundown and Paragon Groups.||Undifferentiated: mostly metasediments and composite gneisses with lesser quartzo-feldspathic and amphibole/pyroxene rich (basic) gneisses.|
20135|Willyama Supergroup|70015|5|Briefly described|Map legend|Statherian|Statherian|Mineral deposits (if any) are shown.|||Includes Curnamona, Rantyga, Thackaringa, Broken Hill, Sundown and Paragon Groups; Thorndale Composite Gneiss; Silver City Suite.||Low to high grade metasedimentary rock, composite gneiss, quartzofeldspathic gneiss, calc-silicate, Zn-, Mn- and Fe-rich rock, foliated granite, pegmatite; amphibolite stratiform or discordant dykes containing plagioclase, amphibole and/or pyroxene.|
20135|Willyama Supergroup|70339|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic||||Mount Howden, Ethiudna Subgroups; Saltbush, Curnamona Groups; George Mine Formation.||Psammopelite; psammite; pelite; metasediments characterised by calc-silicate minerals and alkali feldspar, magnetite- or haematite-bearing; local iron formation, sulphidic metasediments, carbonate rocks.|02-FEB-16
20135|Willyama Supergroup|70340|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic||||||Psammopelite; psammite; pelite; metasediments characterised by calc-silicate minerals and alkali feldspar, magnetite- or haematite-bearing; local iron formation, sulphidic metasediments, carbonate rocks.|
20135|Willyama Supergroup|70383|6|Mentioned|p51|Statherian|Statherian|Mentioned as a possible source of zircons aged c.1670 +/- 24 Ma, extracted from the Sprigg Diamictite Member.||||||
20135|Willyama Supergroup|70405|4|Described|p1,p6,p7,p12 figure 4,p 15, p83, p 86|Mesoproterozoic|Paleoproterozoic|Previously termed Willyama Complex.|1700 Ma -1650 Ma||Includes Curnamona Group, Bimba Formation, Plumbago Formation, Raven Hill Subgroup, Mount Howden Subgroup, Paragon Group, Sundown Group, Broken Hill Group, Thackaringa Group|Intruded by Bimbowrie Suite|Amphibolite facies albitic, siliciclastic and minor calcareous metasediments; Gneisses and migmatites. Numerous mafic dykes.|
20135|Willyama Supergroup|70657|4|Described|p6-17, p21, p28, p32, p42-46, p50-51|Statherian|Statherian|See also p53-54, p58-59, p65, p67, p69, p72. Olary, Mulyungarie and Olary Domains, Curnamona Province. Total thickness unknown: neither top nor base observed; probably c.5km, multiplied by structural repetition. Associated igneous suites include Ninnerie Supersuite, Lady Louise Suite, Basso Suite (all in the Olary Domain); Mundi Mundi Granites, Cusin Creek Granite, Purnamoota Road leucogneiss, Hores Gneiss, Parnell Gneiss, Silver City Suite (all in the Broken Hill Domain). The Arunta terrane may be a source for some of the sediment. The bulk of the metasediments are enriched in HFSE, REE, U and Th up to the Cartwrights Creek Metasediments. Deformation, particularly Delamerian Orogeny, discussed in detail.|1719  - < 1642 +/- 5 Ma.||Includes Sundown, upper Saltbush, Paragon, Strathearn, Thackaringa, Rantyga, Curnamona, Broken Hill Groups.|||
20135|Willyama Supergroup|70658|5|Briefly described|p1-2, 5, 9, 11, 14-16, 32, 47|Paleoproterozoic|Paleoproterozoic|Curnamona Province.|1720-1640 Ma.||Rantyga, Thackaringa Groups.|||
20135|Willyama Supergroup|70659|6|Mentioned|p4|||||||||
20135|Willyama Supergroup|70829|6|Mentioned|p33|Paleoproterozoic|Paleoproterozoic|Curnamona Province. Enhanced conductivity discussed.||||||
20135|Willyama Supergroup|70858|6|Mentioned|p14, 27 Fig.11H, p33-34|Paleoproterozoic|Paleoproterozoic|Curnamona Province. Similar Zr geochronology and Nd isotope ratios suggest a shared depositional system with Tarcoola Formation and Isa Supergroup, and the Wernecke Supergroup of Yukon.|||Sundown Group.|||
20135|Willyama Supergroup|70947|6|Mentioned|p960|Statherian|Statherian|Geological province: Curnamona Province.|ca. 1720-1650 Ma|||||
20135|Willyama Supergroup|71322|5|Briefly described|p38|||Hosts the Cu-Au Kalkaroo deposit.||||||
20135|Willyama Supergroup|71341|6|Mentioned|p179 fig 1|Palaeoproterozoic|Palaeoproterozoic||ca. 1720-1640 Ma|||||
20135|Willyama Supergroup|71799|5|Briefly described|p150 fig 2, p165|Statherian|Statherian|Curnamona Province.|ca 1700 Ma|||||
20135|Willyama Supergroup|71968|5|Briefly described|p1,3-4,6,13,18-19,28,41,45|Paleoproterozoic|Paleoproterozoic|Geological province: Curnamona province .Deformation-related metamorphic assemblages may have been developed during the high-grade Olarian Orogeny during 1620-1580 Ma (Binns, 1964; Hobbs et al., 1984; Clarke et al., 1987; Page and Laing, 1992); most of the assemblages are betwen 1600-1590 Ma (Page et al., 2005a) based on metamorphic zircon, rutile and monazite ages, and syn- to late-tectonic granites (see p7 for references). Barovich and Hand (2008) suggested the NAC was the likely sediment source for the lower Wiillyama Supergroup based on whole rock Sm-Nd data.|||Includes Paragon Group, Sundown Group.|||06-DEC-19
20135|Willyama Supergroup|72004|4|Described|p73,83-90|Statherian|Statherian|Geological province: Olary Block. Broken Hill region. Age from Page et al., 2005. Underwent high-grade metamorphism at c. 1600 Ma (Grew et al., 2012, Page et al., 2005). Contains sodic rocks of possibly evaportic origin and bimodal volcanism, indicative of continental rift deposition.|c. 1700-1685 Ma|||Lithologically similar to prismatine-bearing granulites in the Windmill Islands, Wilkes Land and granulite-facies paragneisses, Larsemann Hills. Underlain by Thackaringa Group.|Metaevaporites, tourmaline-quartz rocks, sodic gneisses and apatitic iron formation|
20135|Willyama Supergroup|72435|6|Mentioned|p715|Palaeoproterozoic|Palaeoproterozoic|Broken Hill.||||||
20135|Willyama Supergroup|72454|5|Briefly described|p1, p2 Fig.2, p7, p12, p20, p25|Mesoproterozoic|Mesoproterozoic|Olary Domain. See also p34, p39, p42 Fig.26, p44, p47, p48 Fig.33, p49, p54. Volcanics were extruded over the eroded surface of the Willyama Supergroup. Bimbowrie Suite granites were largely derived from melting of Willyama Supergroup sediments.|c. 1600 to 1570 Ma.||Includes Paragon Group, Sundown Group, Broken Hill Group, Thackaringa Group, Thorndale Composite Gneiss, Strathearn Group, Curnamona Group.||Includes pelitic and psammopelitic metasediments.|09-SEP-20
20135|Willyama Supergroup|72461|5|Briefly described|p4-5, p13|||Of the  Curnamona Craton. Oldest rocks in NSW.|1700 Ma||Includes the Thackaringa Group, Broken Hill Group, Sundown Group and the Paragon Group.|||
20135|Willyama Supergroup|73021|5|Briefly described|p224-225|||Broken Hill area, SE Curnamona Craton. ~7 km thick. Intracontinental rift setting. Large areas of stratigraphy were inverted by the Olarian Orogeny.|~1710-1704 Ma (middle) to ~1642 Ma (top).||Thackaringa, Broken Hill Groups; Basso Suite.||A wide range of metamorphosed deformed lithologies including pelite, psammopelite, psammite, quartzofeldspathic and mafic rocks and hydrothermal sediments.|
20135|Willyama Supergroup|73030|5|Briefly described|p2147-2153|Statherian|Statherian|Curnamona Province. Oldest exposed rocks in the province. Deposited in a rift basin. Extensively altered by sodic metasomatism, potentially indicative of an evaporitic sedimentary component.|ca. 1710 to 1640 Ma|||||
20135|Willyama Supergroup|73092|6|Mentioned|p5|||Curnamona Province. Deposition was synchronous with that of the metasedimentary protoliths to the Barossa Complex and onset of the Kimban Orogeny in the Gawler Craton.||||||
20135|Willyama Supergroup|73093|5|Briefly described|map legend|Palaeoproterozoic|Paleoproterozoic|Undifferentiated.|||||Schist, gneiss, quartzite, migmatite.|12-DEC-21
20135|Willyama Supergroup|73118|6|Mentioned|p31|||||||||
20135|Willyama Supergroup|73129|6|Mentioned|p43|late Palaeoproterozoic|late Palaeoproterozoic|Curnamona Province|||||metasediments|
20135|Willyama Supergroup|73155|6|Mentioned|P286|||Curnamona Province.||||||
20135|Willyama Supergroup|73162|6|Mentioned|p449, Fig.1|Statherian|Statherian||1720-1640 Ma|||||
20135|Willyama Supergroup|73188|6|Mentioned|p352|Statherian|Statherian|Curnamona Province. Coeval with sedimentary protoliths of the high-grade metamophic basement rocks of the Mount Lofty Ranges (Conor and Preiss, 2008).|1720-1640 Ma|||||
20135|Willyama Supergroup|73235|6|Mentioned|p52|Statherian|Statherian||c. 1720-1650 Ma|||||
20135|Willyama Supergroup|73243|4|Described|p51, p52 Fig.1 p54, p57, p59|Statherian|Statherian|Broken Hill Domain, Broken Hill block-Euriowie block. ~7km-thick sequence. Amphibolite sills and dykes typical of rift tholeiites were emplaced before folding and metamorphism, are confined to the Broken Hill Group and stratigraphically lower groups. Zircon U-Pb dates from amphibolites range from 1674 +/- 8 Ma to 1691 +/- 9 Ma (Gibson and Nutman, 2004), and metamorphic grades range from lower amphibolite to hornblende granulite, produced by the Olarian Orogeny ca 1600 Ma. Amphibolite is used in text to refer to all highly metamorphosed pre-1600 Ma mafic rocks including hornblende granulites and pyroxene granulites. Some amphibolites have very high iron oxide values. Post-metamorphic intrusions include mafic to ultramafic dykes and plugs, minor granite bodies.|1691 +/- 9 Ma, 1674 +/- 8 Ma zircon U-Pb||Clevedale Migmatite, Thorndale Composite Gneiss, Thackaringa Group, Broken Hill Group, Sundown Group, Paragon Group, Rantyga Group||Sequence of metasedimentary rocks with minor metavolcanic units, highly metamorphosed and deformed. Intruded during deposition by abundant amphibolite (meta-dolerite) sills and dykes as well as granite bodies, now granite gneisses.|17-AUG-22
20135|Willyama Supergroup|73244|6|Mentioned|p86||||||||Metasedimentary/igneous[?].|
20135|Willyama Supergroup|73251|6|Mentioned|p36|Statherian|Statherian|Curnamona Province.|c. 1730-1640 Ma|||||
20135|Willyama Supergroup|73308|5|Briefly described|p605-608, 623||||1710-1640 Ma.||Paragon, Broken Hill, Sundown, Rantyga, Thackaringa Groups; Thorndale Composite Gneiss, Clevedale Migmatite.||Metasediments and minor volcanics. Includes mainly metasediments, with granite gneiss and garnet-biotite-rich quartzo-feldspathic gneiss, and sills and dykes of amphibolite and basic granulite.|
20135|Willyama Supergroup|73429|5|Briefly described|p105, p106 Fig.2, p107-108, p114|Statherian|Statherian|Curnamona Province. Deposited in an epi-continental rift basin. Deformed between c. 1610 Ma and c. 1590 Ma. Informally the supergroup is commonly subdivided into lower and upper packages separated by a regionally extensive redox boundary associated with stratiform Cu-Au mineralisation.|c. 1702-1640 Ma||lower Willyama Supergroup, upper Willyama Supergroup||Includes metasediments.|
20135|Willyama Supergroup|73479|6|Mentioned|p155, p156 Fig.2|Precambrian|Precambrian|Basement to Warburton Basin.|||||Meta-sedimentary.|
20135|Willyama Supergroup|73482|5|Briefly described|p419-420, p422 Fig.3, p423, p431|Paleoproterozoic|Paleoproterozoic|Intruded by granites, tholeiitic dolerite/gabbro sills and dykes from 1710 to 1680 Ma. Peak metamorphic grade at about 1600 Ma (SHRIMP U-Pb metamoprhic zircons; Page et al., 2005; Stevens et al., 2008). Ranges from chlorite grade in Euriowie Block, to two-pyroxene granulite grade in the southern Broken Hill Block. In major fold structures the upper stratigraphic units are at lower metamorphic grades.|1720-1640 Ma||Thorndale Composite Gneiss, Thackaringa Group, Broken Hill Group, Sundown Group, Paragon Group, Rantyga Group||Sedimentary-volcanic sequence, metamorphosed.|
20135|Willyama Supergroup|73512|5|Briefly described|p1-3, p7-8|Statherian|Statherian|Curnamona Province, Broken Hill Block. Reflects granulite facies Olarian metamorphism at ca 1600 Ma. Deposited in an intracratonic rift setting. [Informal lower and upper subdivisions are used on p3 and p7].|||Thackaringa Group, Broken Hill Group, Sundown Group, Paragon Group, Clevedale Migmatite, Thorndale Composite Gneiss|||
20135|Willyama Supergroup|73516|5|Briefly described|p2, p6|Statherian|Statherian|Curnamona Province. Commonly subdivided into a lower and upper supergroup. Lower-Middle Willyama Supergroup shown p3 Fig.1.|~1720-1640 Ma|||Intruded by Ninnerie Supersuite|Meta-sedimentary and meta-igneous units.|
20135|Willyama Supergroup|73524|5|Briefly described|p1-4, p19 Fig.17, p20-21|Statherian|Statherian|Curnamona Province. Total thickness estimates range from 8-15 km. Paleo-Mesoproterozoic metamorphic field gradient from greenschist-facies in the NW to granulite-facies in the SE. Early (c.1630 Ma) metamorphism attributed to elevated levels of radiogenic heat production.|1720-1640 Ma||lower Willyama Supergroup|Intruded by Ninnerie Supersuite|Dominated by metasedimentary rocks, including metamorphosed clastic, volcaniclastic, volcanic and intrusive lithologies.|
20135|Willyama Supergroup|73575|5|Briefly described|p825, p828 Fig.2, p833, p835|Paleoproterozoic|Paleoproterozoic||||Thorndale Composite Gneiss, Thackaringa Group, Broken Hill Group, Sundown Group, Paragon Group, Rantyga Group|||
20135|Willyama Supergroup|73600|6|Mentioned|p192|||Broken Hill Provence.||||||
20135|Willyama Supergroup|74367|6|Mentioned|p23|||Curnamona Province.||||||
20148|Wilpena Group|7931|5|Briefly described|p98|Neoproterozoic|Neoproterozoic|Comprises Sandison and Pound Subgroups. Unconformably overlain by the Hawker Group. Max. thickness: 4km.||||||07-FEB-11
20148|Wilpena Group|9862|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Probably includes Wonoka Formation and Brachina Formation. Grey-green laminated siltstone with laminated grey flaggy quartzite and brown-weathering dolomite, marble and sandy marble.||||||
20148|Wilpena Group|22510|5|Briefly described|table1p37|||Age: marinoan. Stuart Shelf||||||
20148|Wilpena Group|22553|6|Mentioned|p77|||part of the Adelaidean sequence||||||
20148|Wilpena Group|22631|5|Briefly described|fig2 p170|Neoproterozoic|Neoproterozoic|||||||
20148|Wilpena Group|22643|6|Mentioned|p186|Proterozoic|Proterozoic|||||||
20148|Wilpena Group|22645|6|Mentioned|Fig4 P204|Cambrian|Proterozoic|||||||
20148|Wilpena Group|22671|6|Mentioned|p850|||||||||
20148|Wilpena Group|22677|5|Briefly described|p733, Fig.2 p735|Neoproterozoic|Neoproterozoic|||||||
20148|Wilpena Group|22725|6|Mentioned|p242 fig1|||||||||
20148|Wilpena Group|22746|6|Mentioned|p513|Neoproterozoic III|Neoproterozoic III|||||||
20148|Wilpena Group|22755|6|Mentioned|p555|||||||||
20148|Wilpena Group|22772|4|Described|p63,Table13.1|Neoproterozoic III|Neoproterozoic III|||||||
20148|Wilpena Group|22857|5|Briefly described|p64, Tb. 13.1 (insert p70-71)|Marinoan|Marinoan|Now included in the Heysen Supergroup and belongs to a new Pangean supercycle (Veevers, 1990). Age: 590-545Ma.||||||
20148|Wilpena Group|22869|6|Mentioned|P37|||||||||
20148|Wilpena Group|22921|5|Briefly described|37|||||||||
20148|Wilpena Group|22926|6|Mentioned|37|||Geol province Adelaide Geosyncline||||||
20148|Wilpena Group|22949|5|Briefly described|p27|Neoproterozoic|Neoproterozoic|||||||
20148|Wilpena Group|23176|6|Mentioned|p12||Neoproterozoic|Adelaide Geosyncline||||||
20148|Wilpena Group|23178|6|Mentioned|Fig.1||Neoproterozoic|||||||
20148|Wilpena Group|23211|6|Mentioned|p40,45 Fig.1,2|||||||||
20148|Wilpena Group|23250|5|Briefly described|p1125 Fig.3||Neoproterozoic III|For correlates see members.||||||
20148|Wilpena Group|23287|6|Mentioned|Fig.3,4|||||||||
20148|Wilpena Group|23315|5|Briefly described|p344|Neoproterozoic|Neoproterozoic|Includes the Brachina, Bunyeroo, Wonoka and Billy Springs Formations, and Pound Quartzite which include a range of lithologies.||||||07-FEB-07
20148|Wilpena Group|23351|5|Briefly described|283|Neoproterozoic|Neoproterozoic|||||||
20148|Wilpena Group|23394|5|Briefly described|Map legend|Proterozoic|Proterozoic|||||||
20148|Wilpena Group|23411|6|Mentioned|Map Legend|||||||||
20148|Wilpena Group|23412|5|Briefly described|Map Legend|Proterozoic|Proterozoic|||||||
20148|Wilpena Group|23445|5|Briefly described|p435|||||||||
20148|Wilpena Group|23557|5|Briefly described|p95 Fig.1|Neoproterozoic III|Neoproterozoic III|Geological Province: Adelaide Rift Complex.||||||
20148|Wilpena Group|23719|5|Briefly described|p26|||Overlain by Kulpara Limestone. Underlain by Umberatana Group. Geological Province: Gawler Craton.||||||24-JUN-09
20148|Wilpena Group|23731|6|Mentioned|p20|Adelaidean|Adelaidean|||||||
20148|Wilpena Group|23805|5|Briefly described|p5 Fig. 3|Neoproterozoic|Neoproterozoic|Includes the Tent Hill Formation.  Geological Province: Gawler Craton.||||||
20148|Wilpena Group|23806|5|Briefly described|p1122 Fig. 1|Neoproterozoic|Neoproterozoic|||||||
20148|Wilpena Group|23818|5|Briefly described|p34 Fig.8|Adelaidean|Adelaidean|Geological Province: Willyama Block. Max. thickness: 20 000 ft.||||||
20148|Wilpena Group|23854|5|Briefly described|p863|||||||||
20148|Wilpena Group|23869|5|Briefly described|p14|Neoproterozoic|Neoproterozoic|||||||
20148|Wilpena Group|23913|4|Described|p110 Fig. 2|Adelaidean|Adelaidean|Geological Province: Adelaide Geosyncline.  Underlain by Umberatana Group.||||||11-SEP-07
20148|Wilpena Group|24045|5|Briefly described|p533 Fig.2|Adelaidean|Adelaidean|||||||
20148|Wilpena Group|24175|4|Described|p13|Neoproterozoic|Neoproterozoic|Of Heysen Supergroup. Max. Thickness: 1640m.||||||
20148|Wilpena Group|24176|3|Fully described|p13, p24 Tb. 1|Adelaidean|Adelaidean|Overlies the Umberatana Group. Age is Marinoan. Geological Province: Mount Painter Province.||||||06-FEB-08
20148|Wilpena Group|24261|5|Briefly described|p1047 Fig.1|Neoproterozoic|Neoproterozoic|Geological Province: Gawler Craton||||||
20148|Wilpena Group|24321|5|Briefly described|Map legend|Late Adelaidean|Late Adelaidean|||||||
20148|Wilpena Group|24400|5|Briefly described|p155 Tb.2|Adelaidean|Adelaidean|Overlies Umberataana Group.||||||03-MAR-05
20148|Wilpena Group|24481|5|Briefly described|p829 Fig. 9|||Overlies the Umberatana Group. Overlain by the Parachilna Formation.||||||
20148|Wilpena Group|24484|5|Briefly described|p798 Fig. 1|Neoproterozoic|Neoproterozoic|||||||
20148|Wilpena Group|24546|5|Briefly described|p2 - 3 Fig.2|Neoproterozoic|Neoproterozoic|Age: ~620-550 Ma. Geological Province: Adelaide Fold Belt.||||||16-JAN-08
20148|Wilpena Group|24586|5|Briefly described|p50 Fig. 1, p51 Fig. 2|Adelaidean|Adelaidean|Of the Heysen Supergroup. Includes Sandison, Aruhna, Depot Springs and Pound Subgroups. Geological Province: Adelaide Geosyncline.||||||09-MAY-16
20148|Wilpena Group|24593|5|Briefly described|p612 Fig. 1a|||Geological Province: Mount Painter Inlier.||||||
20148|Wilpena Group|29656|6|Mentioned|Fig.9|||||||||
20148|Wilpena Group|29697|6|Mentioned|p7|||||||||
20148|Wilpena Group|29780|6|Mentioned|p42|||||||||
20148|Wilpena Group|29781|6|Mentioned|p47|||||||||
20148|Wilpena Group|29834|6|Mentioned|p198|||||||||
20148|Wilpena Group|29837|4|Described|p75|||||||||
20148|Wilpena Group|29838|6|Mentioned|p4|||||||||
20148|Wilpena Group|29840|6|Mentioned|Fig.3|||||||||
20148|Wilpena Group|29929|6|Mentioned|Fig.1|||||||||
20148|Wilpena Group|30028|6|Mentioned|Fig.4|||||||||
20148|Wilpena Group|30049|5|Briefly described|p43|||Proterozoic (Marinoan) age.||||||
20148|Wilpena Group|30052|6|Mentioned|Fig.3|||Proterozoic age.||||||
20148|Wilpena Group|30176|6|Mentioned|Map legend|Adelaidean|Adelaidean|Marinoan||||||
20148|Wilpena Group|30177|4|Described|p88|||Marinoan age. See also p89-92.||||||11-SEP-07
20148|Wilpena Group|30190|6|Mentioned|Fig.1|||||||||
20148|Wilpena Group|30261|6|Mentioned|Table 1|||Marinoan age||||||
20148|Wilpena Group|30621|6|Mentioned|p501|||||||||
20148|Wilpena Group|30798|6|Mentioned|p116|||||||||
20148|Wilpena Group|30800|6|Mentioned|p219|||||||||
20148|Wilpena Group|30801|6|Mentioned|p5|||Marinoan. Table P5-6||||||
20148|Wilpena Group|30802|4|Described|p12|||Adelaidean||||||
20148|Wilpena Group|30807|6|Mentioned|p102|||Suggested map symbol||||||
20148|Wilpena Group|30808|6|Mentioned|Fig.1|||||||||
20148|Wilpena Group|30810|6|Mentioned|Fig.1|||||||||
20148|Wilpena Group|30917|6|Mentioned|p38|||||||||
20148|Wilpena Group|30923|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
20148|Wilpena Group|31022|6|Mentioned|Fig. 4|||||||||
20148|Wilpena Group|31109|6|Mentioned|p32|||See also P34, 36. Map.||||||
20148|Wilpena Group|31719|6|Mentioned|p17|||Marinoan. Refers Johns (1968)||||||
20148|Wilpena Group|31730|6|Mentioned|p99|||U.Proterozoic. Geochem. Stream Sediment sampling||||||
20148|Wilpena Group|31797|6|Mentioned|p131|||Adelaidean||||||
20148|Wilpena Group|31826|6|Mentioned|p33|||||||||
20148|Wilpena Group|31923|6|Mentioned|p8|||||||||
20148|Wilpena Group|31965|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
20148|Wilpena Group|32144|6|Mentioned|p81|||Organic matter||||||
20148|Wilpena Group|32146|6|Mentioned|p349|||Refers Thomson et at. (1964)||||||
20148|Wilpena Group|32504|6|Mentioned|Fig.2|||||||||
20148|Wilpena Group|32505|6|Mentioned|Table 3|||||||||
20148|Wilpena Group|32511|6|Mentioned|p13|||||||||
20148|Wilpena Group|32547|6|Mentioned|p60|||Marinoan||||||
20148|Wilpena Group|32720|6|Mentioned|Table 1|||Late Adelaidean||||||
20148|Wilpena Group|32722|6|Mentioned|Fig.3|||Adelaidean. Stromatolite||||||
20148|Wilpena Group|32724|6|Mentioned|Fig.1|||Correlation||||||
20148|Wilpena Group|32791|6|Mentioned|p11|||||||||
20148|Wilpena Group|33004|6|Mentioned|p136|||||||||
20148|Wilpena Group|33035|6|Mentioned|p53|||||||||
20148|Wilpena Group|33036|6|Mentioned|p18|||||||||
20148|Wilpena Group|33037|6|Mentioned|Fig.2|||||||||
20148|Wilpena Group|33210|6|Mentioned|Fig.1|||||||||
20148|Wilpena Group|33422|6|Mentioned|Map legend|Precambrian|Precambrian|||||||
20148|Wilpena Group|33423|4|Described|p13|||||||||
20148|Wilpena Group|33474|6|Mentioned|Fig.2|||||||||
20148|Wilpena Group|33490|6|Mentioned|p11|||Stratigraphy||||||
20148|Wilpena Group|33551|6|Mentioned|Fig.1|||Proterozoic||||||
20148|Wilpena Group|33655|6|Mentioned|p91|||||||||
20148|Wilpena Group|33692|6|Mentioned|p162|||U.Prot.||||||
20148|Wilpena Group|33693|6|Mentioned|p153|||||||||
20148|Wilpena Group|33932|6|Mentioned|Fig.2|||||||||
20148|Wilpena Group|33934|6|Mentioned|Fig.2|||U. Prot.||||||
20148|Wilpena Group|33953|6|Mentioned|Fig.4|||Proterozoic||||||
20148|Wilpena Group|33954|6|Mentioned|p97|||See also Fig.4||||||
20148|Wilpena Group|33955|6|Mentioned|Fig.2|||Camb.||||||
20148|Wilpena Group|33957|6|Mentioned|p36|||||||||
20148|Wilpena Group|34014|5|Briefly described|p22|||Proterozoic||||||
20148|Wilpena Group|34069|6|Mentioned|p4|||||||||
20148|Wilpena Group|34116|6|Mentioned|p20|||||||||
20148|Wilpena Group|34175|5|Briefly described|p37|||||||||
20148|Wilpena Group|34202|6|Mentioned|p1058|||Precambrian||||||
20148|Wilpena Group|34287|6|Mentioned|p40|||See also P42||||||
20148|Wilpena Group|34291|6|Mentioned|p11|||Adelaidean. See also P17||||||
20148|Wilpena Group|34318|6|Mentioned|p86|||||||||
20148|Wilpena Group|34483|6|Mentioned|p113|||||||||
20148|Wilpena Group|34534|6|Mentioned|Fig.2.13|||||||||
20148|Wilpena Group|34535|4|Described|p72|||Marinoan Fig.16.||||||11-SEP-07
20148|Wilpena Group|34536|6|Mentioned|Map legend|Adelaidean|Adelaidean|Marinoan||||||
20148|Wilpena Group|34537|6|Mentioned|Fig.8|||||||||
20148|Wilpena Group|34563|6|Mentioned|p67|||Stratigraphy and correlation||||||
20148|Wilpena Group|34611|6|Mentioned|p153|||||||||
20148|Wilpena Group|34612|6|Mentioned|Fig.40|||Adelaidean||||||
20148|Wilpena Group|34766|6|Mentioned|Fig.2|||||||||
20148|Wilpena Group|34812|6|Mentioned|p4|||||||||
20148|Wilpena Group|34833|6|Mentioned|p76|||||||||
20148|Wilpena Group|34835|6|Mentioned|Fig.2|||||||||
20148|Wilpena Group|34836|6|Mentioned|Fig.2|||||||||
20148|Wilpena Group|34844|6|Mentioned|p98|||||||||
20148|Wilpena Group|34901|6|Mentioned|p18|||||||||
20148|Wilpena Group|34911|6|Mentioned|p86|||||||||
20148|Wilpena Group|35002|6|Mentioned|p28|||||||||
20148|Wilpena Group|35075|6|Mentioned|p77|||||||||
20148|Wilpena Group|35143|6|Mentioned|Fig.2|||||||||
20148|Wilpena Group|35158|6|Mentioned|p47|||||||||
20148|Wilpena Group|35195|6|Mentioned|Table 3|||||||||
20148|Wilpena Group|35217|6|Mentioned|p179|||||||||
20148|Wilpena Group|35255|5|Briefly described|p13|||See also Fig.3.||||||
20148|Wilpena Group|35270|6|Mentioned|Fig.2|||||||||
20148|Wilpena Group|35327|6|Mentioned|Fig.1|||||||||
20148|Wilpena Group|35356|6|Mentioned|p29|||||||||
20148|Wilpena Group|35543|6|Mentioned|Fig.1|||Regional bedrock geology.||||||
20148|Wilpena Group|35548|6|Mentioned|p17|||||||||
20148|Wilpena Group|35582|6|Mentioned|Fig.2|||||||||
20148|Wilpena Group|35586|6|Mentioned|p25|||Suggested to be subgroup status||||||
20148|Wilpena Group|35675|6|Mentioned|Fig.1|||Location plan & regional geology.||||||
20148|Wilpena Group|35954|6|Mentioned|Fig.2|||||||||
20148|Wilpena Group|36003|6|Mentioned|p1030|||||||||
20148|Wilpena Group|36081|6|Mentioned|Fig.1|||||||||
20148|Wilpena Group|36083|6|Mentioned|Table 1|||||||||
20148|Wilpena Group|36126|6|Mentioned|Fig.1|||||||||
20148|Wilpena Group|36137|6|Mentioned|p4|||||||||
20148|Wilpena Group|36198|6|Mentioned|Fig.I.2|||||||||
20148|Wilpena Group|36212|5|Briefly described|p3|||||||||
20148|Wilpena Group|36245|6|Mentioned|p5|||||||||
20148|Wilpena Group|36514|6|Mentioned|p55|||||||||
20148|Wilpena Group|36622|6|Mentioned|Fig.2|||||||||
20148|Wilpena Group|36731|4|Described|p124|||||||||
20148|Wilpena Group|36833|6|Mentioned|Fig.1|||||||||
20148|Wilpena Group|36839|6|Mentioned|Fig.2|||||||||
20148|Wilpena Group|36898|6|Mentioned|p182|||See also P196.||||||
20148|Wilpena Group|36966|6|Mentioned|Fig.1|||||||||
20148|Wilpena Group|37015|6|Mentioned|Fig.2|||||||||
20148|Wilpena Group|37113|6|Mentioned|Fig.1|||||||||
20148|Wilpena Group|37238|6|Mentioned|Table 1|||||||||
20148|Wilpena Group|37461|6|Mentioned|Fig.5.10|||||||||
20148|Wilpena Group|37462|6|Mentioned|p294|||||||||
20148|Wilpena Group|37627|6|Mentioned|p186|||||||||
20148|Wilpena Group|37927|6|Mentioned|p507|||||||||
20148|Wilpena Group|38004|6|Mentioned|p82|||See also Table 1.||||||
20148|Wilpena Group|38022|6|Mentioned|p48|||||||||
20148|Wilpena Group|38068|4|Described|p68|||See also Fig.4.||||||
20148|Wilpena Group|38110|6|Mentioned|p2|||||||||
20148|Wilpena Group|38157|6|Mentioned|Table 1|||||||||
20148|Wilpena Group|38243|6|Mentioned|p359|||||||||
20148|Wilpena Group|38330|6|Mentioned|p217|||||||||
20148|Wilpena Group|38581|6|Mentioned|p252|||||||||
20148|Wilpena Group|38703|6|Mentioned|p131|||||||||
20148|Wilpena Group|38704|6|Mentioned|p133|||||||||
20148|Wilpena Group|38970|6|Mentioned|p105|||||||||
20148|Wilpena Group|39047|6|Mentioned|Table 2|||||||||
20148|Wilpena Group|39210|6|Mentioned|Table 3|||||||||
20148|Wilpena Group|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Marinoan||||||
20148|Wilpena Group|39349|6|Mentioned|Map legend|Adelaidean|Adelaidean|Marinoan||||||
20148|Wilpena Group|39351|6|Mentioned|Map legend|Adelaidean|Adelaidean|Marinoan||||||
20148|Wilpena Group|39352|6|Mentioned|Map legend|Adelaidean|Adelaidean|Marinoan||||||
20148|Wilpena Group|39490|6|Mentioned|Fig.1(6)|||||||||
20148|Wilpena Group|39526|6|Mentioned|p684|||||||||
20148|Wilpena Group|39635|6|Mentioned|Fig.2|||||||||
20148|Wilpena Group|39675|6|Mentioned|p180|||||||||
20148|Wilpena Group|39724|6|Mentioned|Fig.6|||||||||
20148|Wilpena Group|39762|6|Mentioned|Table 1|||||||||
20148|Wilpena Group|39802|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
20148|Wilpena Group|39807|6|Mentioned|p225|||||||||
20148|Wilpena Group|39808|6|Mentioned|p223|||||||||
20148|Wilpena Group|39885|6|Mentioned|p427|||||||||
20148|Wilpena Group|40105|6|Mentioned|p313|||See also Fig.3||||||
20148|Wilpena Group|40228|6|Mentioned|p38|||||||||
20148|Wilpena Group|40257|6|Mentioned|Fig.2|||||||||
20148|Wilpena Group|40294|6|Mentioned|p54|||||||||
20148|Wilpena Group|40442|4|Described|p10|||||||||
20148|Wilpena Group|40455|6|Mentioned|Fig.2|||||||||
20148|Wilpena Group|40456|5|Briefly described|p19|||||||||
20148|Wilpena Group|40537|6|Mentioned|p350|||||||||
20148|Wilpena Group|40595|6|Mentioned|Fig.8|||||||||
20148|Wilpena Group|40720|5|Briefly described|p55|||||||||
20148|Wilpena Group|40852|6|Mentioned|p29|||See also P32||||||
20148|Wilpena Group|40906|6|Mentioned|Fig.9|||||||||
20148|Wilpena Group|40914|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
20148|Wilpena Group|41005|6|Mentioned|p417|||||||||
20148|Wilpena Group|41085|6|Mentioned|Fig.7|||||||||
20148|Wilpena Group|41236|5|Briefly described|p60|||||||||
20148|Wilpena Group|41256|6|Mentioned|p7|||||||||
20148|Wilpena Group|41364|6|Mentioned|Fig.1|||||||||
20148|Wilpena Group|41400|6|Mentioned|p23|||||||||
20148|Wilpena Group|41401|6|Mentioned|p29|||||||||
20148|Wilpena Group|41429|4|Described|p211|||See also p218.||||||11-SEP-07
20148|Wilpena Group|41493|5|Briefly described|Table 2|||||||||
20148|Wilpena Group|41495|5|Briefly described|p44|||||||||
20148|Wilpena Group|41496|6|Mentioned|p52|||||||||
20148|Wilpena Group|41500|6|Mentioned|p79|||||||||
20148|Wilpena Group|41526|6|Mentioned|p14|||||||||
20148|Wilpena Group|41647|6|Mentioned|Fig.2|||||||||
20148|Wilpena Group|41770|6|Mentioned|Fig.1|||||||||
20148|Wilpena Group|41794|6|Mentioned|p790|||See also Fig.2||||||
20148|Wilpena Group|42028|6|Mentioned|p137|||||||||
20148|Wilpena Group|42087|5|Briefly described|Fig.2 P15|||||||||
20148|Wilpena Group|42088|5|Briefly described|Fig.3 P546|||||||||
20148|Wilpena Group|42090|6|Mentioned|p24|||||||||
20148|Wilpena Group|42095|5|Briefly described|p30|||See also Fig.3||||||
20148|Wilpena Group|42096|6|Mentioned|p37|||||||||
20148|Wilpena Group|42098|4|Described|p51|||||||||
20148|Wilpena Group|42167|6|Mentioned|Fig.2 P115|||||||||
20148|Wilpena Group|42215|6|Mentioned|Fig.2 P448|||||||||
20148|Wilpena Group|42222|4|Described|p15|||See also p18.||||||11-SEP-07
20148|Wilpena Group|42235|4|Described|p140|||||||||
20148|Wilpena Group|42237|6|Mentioned|Fig.6 P90|||||||||
20148|Wilpena Group|42238|4|Described|p77|||||||||
20148|Wilpena Group|42239|6|Mentioned|p158|||||||||
20148|Wilpena Group|42240|6|Mentioned|Fig.2 P165|||||||||
20148|Wilpena Group|42241|6|Mentioned|p178|||||||||
20148|Wilpena Group|42243|4|Described|p211|||||||||
20148|Wilpena Group|42247|6|Mentioned|p9|||||||||
20148|Wilpena Group|42266|6|Mentioned|Fig.2 P292|||||||||
20148|Wilpena Group|42271|6|Mentioned|p372|||||||||
20148|Wilpena Group|42272|6|Mentioned|Fig.2 P400|||||||||
20148|Wilpena Group|42346|5|Briefly described|p77|Adelaidean||||||||
20148|Wilpena Group|42357|6|Mentioned|p10|||||||||
20148|Wilpena Group|42410|5|Briefly described|p2|||||||||
20148|Wilpena Group|42465|5|Briefly described|Map legend|||||||||
20148|Wilpena Group|42469|4|Described|p22|||Stuart Shelf.||||||13-FEB-08
20148|Wilpena Group|42505|5|Briefly described|Map legend|Adelaidean (Marinoan)||||||||
20148|Wilpena Group|42542|6|Mentioned|p8|||||||||
20148|Wilpena Group|42544|5|Briefly described|Fig.1 P17|||||||||
20148|Wilpena Group|42546|5|Briefly described|Map legend|Adelaidean (Marinoan)||||||||
20148|Wilpena Group|42573|5|Briefly described|Fig.1 P190|||||||||
20148|Wilpena Group|42600|5|Briefly described|p6, Table 1|||||||||
20148|Wilpena Group|42643|6|Mentioned|Fig.4 P19|||||||||
20148|Wilpena Group|42720|5|Briefly described|map legend|Marinoan||||||||
20148|Wilpena Group|42721|5|Briefly described|map legend|Marinoan||||||||
20148|Wilpena Group|42723|5|Briefly described|map legend|Marinoan||||||||
20148|Wilpena Group|42736|5|Briefly described|map legend|Neoproterozoic||||||||
20148|Wilpena Group|42763|6|Mentioned|p22|||||||||
20148|Wilpena Group|42813|4|Described|p21|||||||||
20148|Wilpena Group|42882|5|Briefly described|Table 1 P3, Fig7 P12|||of Heysen Supergroup||||||
20148|Wilpena Group|43052|4|Described|p192,Table 6.1|||||||||
20148|Wilpena Group|43053|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Dominantly marine shale, siltstone, sandstone and limestone.||||||26-MAY-05
20148|Wilpena Group|43094|6|Mentioned|p35|||||||||
20148|Wilpena Group|43190|5|Briefly described|p29, Fig.2.|||||||||
20148|Wilpena Group|43258|5|Briefly described|Map Legend||Neoproterozoic|||||||
20148|Wilpena Group|43298|5|Briefly described|Map Legend||Adelaidean|||||||
20148|Wilpena Group|43390|14|Not recorded|p3,diag.p8,9||Proterozoic|Marinoan||||||
20148|Wilpena Group|43595|5|Briefly described|p545||Neoproterozoic|||||||
20148|Wilpena Group|43622|4|Described|p37-39|Early Cambrian|Neoproterozoic|||||||
20148|Wilpena Group|43742|6|Mentioned|p37||Neoproterozoic|||||||
20148|Wilpena Group|43759|6|Mentioned|p450||Adelaidean|||||||
20148|Wilpena Group|43845|5|Briefly described|p41-43,46||Neoproterozoic|See also fig2:p42, fig3:p43||||||12-JUL-16
20148|Wilpena Group|44111|6|Mentioned|p.58 Fig. 2|||in Adelaide Geosyncline||||||
20148|Wilpena Group|44133|5|Briefly described|p46, 51 Fig. 7.18|Adelaidian|Adeladian|Siltstone, quartzite, limestone.||||||
20148|Wilpena Group|44538|4|Described|map legend|||(H53-16). Geol.Atlas Series. Equivalents. Marinoan.||||||
20148|Wilpena Group|44659|5|Briefly described|map legend|||Marinoan, lithology.||||||
20148|Wilpena Group|44660|14|Not recorded|map legend|||Marinoan, lithology.||||||
20148|Wilpena Group|44689|14|Not recorded|map legend|||Andamooka. (H53-12).||||||
20148|Wilpena Group|44690|4|Described|map legend|||Geol. Atlas Series. (I/54-5). Marinoan.||||||
20148|Wilpena Group|44934|5|Briefly described|Map Legend||Adelaidean|||||||
20148|Wilpena Group|45155|6|Mentioned|Fig.7|||Adelaide geosyncline||||||
20148|Wilpena Group|47012|6|Mentioned|p332|||||||||
20148|Wilpena Group|50327|6|Mentioned|p300, p307|Neoproterozoic|Neoproterozoic|Within the Adelaide Rift Complex of South Australia. References to correlations with Tasmanian units.||||||07-FEB-11
20148|Wilpena Group|60418|6|Mentioned|p134 Fig.1|Neoproterozoic|Neoproterozoic|||||||
20148|Wilpena Group|60712|5|Briefly described|p28 Fig. 1|Adelaidean|Adelaidean|Geological Province: Adelaidean Geosyncline.||||||31-MAY-05
20148|Wilpena Group|60718|5|Briefly described|p48 Fig. 1, p49 Fig. 2|Adelaidean|Adelaidean|Geological Province: Adelaide Geosyncline. See also p51 Fig. 3.|||Includes Sandison Subgroup.|||15-APR-11
20148|Wilpena Group|60889|5|Briefly described|p247 Fig.4, p250 Fig.7|Neoproterozoic|Neoproterozoic|Arrowie Basin. Stuart Shelf.||||Unconformably overlain by Uratanna Formation and Parachilna Formation.||22-SEP-17
20148|Wilpena Group|60953|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Dominatly marine shale, siltstone, sandstone and limestone.||||||
20148|Wilpena Group|60955|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Includes Yarloo Shale, Tent Hill Formation, Nuccaleena Formation.||||||
20148|Wilpena Group|60959|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Of the Heysen Supergroup.||||||
20148|Wilpena Group|61108|5|Briefly described|map legend|Adelaidean|Adelaidean|Dominantly marine shale, siltstone, sandstone and limestone.||||||
20148|Wilpena Group|61238|5|Briefly described|p44 Fig. 1|Neoproterozoic|Neoproterozoic|||||||
20148|Wilpena Group|61307|5|Briefly described|p5|||Of the Burra Group. Geological Province: Adelaide Fold Belt.||||||
20148|Wilpena Group|61308|5|Briefly described|p6|Adelaidean|Adelaidean|Quartzite, sandstone, siltstone and limestone.||||||
20148|Wilpena Group|61732|5|Briefly described|p3 Fig. 2, p4 Fig. 3|Marinoan|Marinoan|Includes the Pound and Sandison Subgroups; and the 588+/-35Ma Yarloo Shale. Geological Province: Adelaide Rift Complex/Stuart Shelf.||||||07-FEB-11
20148|Wilpena Group|62085|4|Described|throughout|Neoproterozoic|Neoproterozoic|Flinders Ranges. 3 km thick. Upper part (esp. Pound Subgroup) hosts the Ediacara fauna.|||Pound Subgroup; Wonoka, Bunyeroo, Brachina, Nuccaleena Formations; Rawnsley, ABC Range Quartzites; Bonney Sandstone.|||
20148|Wilpena Group|62453|6|Mentioned|p11 Fig. 7, 12 Fig. 8|Ediacaran|Ediacaran|Geological Province: Adeliade Rift Complex/Stuart Shelf.||||||
20148|Wilpena Group|62592|5|Briefly described|p20 Fig.2.4, p50 Table 5.1, pp58-59.|Ediacaran|Ediacaran|Base of this unit represents Marinoan post-glacial transgression. Very thick in Flinders Ranges. Colour scheme shown for interpretation of Curnamona seismic sections.||Unit in Heysen Supergroup.|Includes Sandison Subgroup, Bunyeroo and Wonoka Formations, Bonney Sandstone and Rawnsley Quartzite.|Disconformably overlies Umberatana Group. Is disconformably overlain by Hawker Group.||
20148|Wilpena Group|62664|5|Briefly described|p138 Fig.2.|Neoproterozoic|Neoproterozoic|||Unit in upper Heysen Supergroup.|Includes Pound Subgroup.|Unconformably overlies Umberatana Group. Is unconformably overlain by Hawker and Normanville Groups.|Sandstone, siltstone and shale, carbonates.|
20148|Wilpena Group|62724|6|Mentioned|p22|||Geological Province: Adelaide Geosycline.||||||07-FEB-11
20148|Wilpena Group|62784|5|Briefly described|p8 Fig.1|Neoproterozoic|Neoproterozoic|Includes Bunyeroo Formation, Wonoka Formation. Underlies Pound Group.||||||
20148|Wilpena Group|62962|5|Briefly described|p2284 Fig. 2|Adelaidean|Adelaidean|Age: 588+/-35Ma and 556+/-24Ma (Preiss, 2000). Geological Province: Mount Painter Province.||||||07-FEB-11
20148|Wilpena Group|63020|5|Briefly described|p973|Neoproterozoic|Neoproterozoic|||||||
20148|Wilpena Group|63458|6|Mentioned|p897 Fig.19. |Ediacaran|Ediacaran|Adelaide Geosyncline.|||Includes Pound Subgroup; Nuccaleena, Brachina, Bunyeroo and Wonoka Formations; Seacliff Sandstone; Ulupa Siltstone; ABC Range Quartzite.|Overlies Umberatana Group. Is overlain by Hawker Group.||
20148|Wilpena Group|63489|5|Briefly described|Map legend|Adelaidean|Adelaidean|Siltstone and sandstone with minor carbonates. New South Wales equivalent is Farnell Group.||||||10-SEP-07
20148|Wilpena Group|63569|6|Mentioned|pp117-118|Neoproterozoic|Neoproterozoic||||Includes Wonoka Formation.|||
20148|Wilpena Group|63811|6|Mentioned|p503|Neoproterozoic|Neoproterozoic|Stuart Shelf.|||Includes ABC Range Quartzite, Bunyeroo Formation.|||28-MAR-12
20148|Wilpena Group|64319|5|Briefly described|p354, p356 Fig.2, p357 Fig.3  |Neoproterozoic|Neoproterozoic|||||Overlies Umberatana Group. Is overlain by Parachilna Formation.|Quartzites, shales and dolomites.|
20148|Wilpena Group|64400|5|Briefly described|p4|||In the Adelaide Rift Complex. Contains the Brachina Formation.||||||07-FEB-11
20148|Wilpena Group|64455|5|Briefly described|p138 Fig. 1|Early Cambrian|Cryogenian|Includes units of Sandison and Pound Subgroups.||||||29-JAN-09
20148|Wilpena Group|64647|5|Briefly described|p38 Fig. 1, p40|Adelaidean|Adelaidean|Overlies Burra Group. Marine sediments.||||||
20148|Wilpena Group|64696|5|Briefly described|p133 Fig.14|Adelaidean|Adelaidean|||||||
20148|Wilpena Group|64724|6|Mentioned|p49 Fig. 7|Ediacaran|Ediacaran|Deposited in the Adelaide Geosyncline during (and slightly before) the Centralian 3 event (~600-544 Ma)||||||02-APR-12
20148|Wilpena Group|64797|5|Briefly described|p151, p153 Fig.2, p160 Fig.8.|Ediacaran|Ediacaran|See also p161, p164 Fig.10, p167 Tb.9. Adelaide Rift Complex.||||||
20148|Wilpena Group|64801|6|Mentioned|p110-111|Neoproterozoic|Neoproterozoic|Adelaide Rift Complex. Contains two thick transgressive-regressive cycles, one siliciclastic and the other mainly carbonate.||Heysen Supergroup.||Overlies Umberatana Group.||
20148|Wilpena Group|64846|6|Mentioned|p197 Fig.2, p198 Fig.3, p199 Fig.4  |Ediacaran|Ediacaran|||||||
20148|Wilpena Group|65365|5|Briefly described|p10 Fig. 4|Ediacaran|Ediacaran|Adelaide Rift Complex / Stuart Shelf. Includes Yarloo Shale dated at 588 +/- 35 Ma, Rb/Sr. Includes Acanthomorph acritarchs.||||||19-MAR-12
20148|Wilpena Group|65366|5|Briefly described|p23 Fig. 3|Ediacaran|Ediacaran|Adelaide Rift Complex / Stuart Shelf. Includes Yarloo Shale dated at 588 +/- 35 Ma, Rb/Sr. Includes Acanthomorph acritarchs.||||||19-MAR-12
20148|Wilpena Group|65376|6|Mentioned|p92 Fig. 2.82. |Neoproterozoic|Neoproterozoic|||||||
20148|Wilpena Group|65483|6|Mentioned|p19|Neoproterozoic|Neoproterozoic|Includes Tent Hill Formation||||||
20148|Wilpena Group|65493|6|Mentioned|p908, 909 Fig 1,2, p921 Fig 14|Ediacaran|Ediacaran|Ediacaran age. Adelaidian units of the Flinders Ranges.||||||
20148|Wilpena Group|65664|6|Mentioned|p1106 Fig.5||||||Includes Brachina Formation.|Unconformably overlain by Normanville Group.||09-MAY-12
20148|Wilpena Group|65892|5|Briefly described|p9 Fig.4, p33-35. |Late Neoproterozoic|Late Neoproterozoic|Arrowie Basin. Contains abundant acritarchs, useful for world-wide Ediacaran correlation.|||Includes Nuccaleena, Brachina, Bunyeroo and Wonoka Formations; ABC Range and Rawnsley Quartzites; Bonney Sandstone.|||
20148|Wilpena Group|65925|5|Briefly described|p14 Fig.2.2, Appendix 2.|Neoproterozoic|Neoproterozoic||||||Quartzite; siltstone; shale; calcareous in part.|
20148|Wilpena Group|66464|5|Briefly described|p167, p168 Fig.2|Ediacaran|Ediacaran|Adelaide Rift Complex. Post-glacial sequences containing sandstone, siltstone, shale and dolomite. Ediacaran biota.||||||
20148|Wilpena Group|66518|6|Mentioned|p19 Fig.4.|Neoproterozoic|Neoproterozoic|Coombalarnie Platform.||||Unconformably overlies Umberatana Group.||
20148|Wilpena Group|66569|5|Briefly described|p860, p861 fig.2,|Ediacaran|Ediacaran|Includes Rawnsley and ABC Range Quartzites; Bonney and Seacliff Sandstones; Wonoka, Bunyeroo, Brachina, Nuccaleena Formations. Unconformably overlies Yerelina Subgroup; unconformably underlies Uratanna Formation.||||||
20148|Wilpena Group|66623|6|Mentioned|p14.|||Correlative of Farnell Group.||||||
20148|Wilpena Group|67127|6|Mentioned|p104|Neoproterozoic|Neoproterozoic|South Australia.|||Includes the Arcoona Quartzite Member, Corraberra Sandstone Member and the Tregolana Shale Member.|Unconformably overlain by the Andamooka Limestone.||
20148|Wilpena Group|67180|5|Briefly described|p600, p601 Fig.1|Neoproterozoic|Neoproterozoic|Established by Thomson et al (1964).||||Overlies the Umberatana Group.||
20148|Wilpena Group|67484|5|Briefly described|p294 Tb.1|Ediacaran|Ediacaran|Adelaide Rift Complex.|||Includes Pound Subgroup; Wonoka, Bunyeroo and Brachina Formations; ABC Range Quartzite.|Overlies Umberatana Group. Is overlain by Hawker Group.||
20148|Wilpena Group|67536|6|Mentioned|Map Legend||||||||Dominantly marine shale, siltstone, sandstone (metazoan fossils) and limestone; deltaic sandstone.|
20148|Wilpena Group|67620|5|Briefly described|p5, 22|Ediacaran|Ediacaran|Adelaide Rift Complex.|||Pound Subgroup; Brachina, Bunyeroo, Wonoka Formations; ABC Range Quartzite.|Overlies Umberatana Group. Is overlain by Hawker Group.||
20148|Wilpena Group|67870|5|Briefly described|p5, p9-10, p13, p17-18, p20-21, p24-25|Neoproterozoic|Neoproterozoic|See also p29-30, p32-34. Adelaide Rift System. Has an erosional upper surface. Produces indistinct sets of low amplitude, discontinuous seismic reflections. Potential hydrocarbon reservoir.|||Sandison, Pound Subgroups; Bunyeroo, Wonoka Formations.||Sandstone, dolostone, siltstone, shale.|
20148|Wilpena Group|67921|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Shown only in section as Wilpena Group equivalents.||||Equivalent to Punkerri Sandstone, Ungoolya Group (Rodda beds) including Karlaya Limestone, Wright Hill beds.|Marine sandstone, grey indurated mudstone and limestone.|
20148|Wilpena Group|67979|5|Briefly described|p528, p530 Fig.1|Neoproterozoic|Neoproterozoic|The Adelaide Geosyncline basinal succession consists of four major lithostratigraphic groups, from base: Callanna, Burra, Umberatana and Wilpena Groups. Geol. Prov: Adelaide Geosyncline (as defined by Thomson et al. 1964 and subsequent revisions)||||Overlies Umberatana Group; is overlain by Hawker Group||22-SEP-14
20148|Wilpena Group|68030|3|Fully described|p236-239|Cambrian|Neoproterozoic|Flinders Ranges. Period of siliciclastic sedimentation that continued into the earliest Cambrian. Characterised by repeated erosional incisions followed by a rapid local rise in sea level.||Unit of Heysen Supergroup.|Includes Wonoka Formation, Bunyeroo Formation, ABC Range Quartzite, Brachina Formation and Nuccaleena Formation.|||26-JUN-19
20148|Wilpena Group|68138|6|Mentioned|p156|Neoproterozoic|Neoproterozoic|Adelaide Rift Complex.|||Brachina, Bunyeroo, Wonoka Formations; ABC Range Quartzite.|||
20148|Wilpena Group|68241|6|Mentioned|p19|||||||Underlain by the Nuccaleena Dolomite.||
20148|Wilpena Group|68269|6|Mentioned|p673-674|||Adelaide Geosyncline. Deposited in low palaeolatitudes.|||Rawnsley Quartzite, Bonney Sandstone, Wonoka Formation, Bunyeroo Formation, ABC Range Quartzite, Brachina Formation, Nuccaleena Formation, Seacliff Sandstone|Underlain by Elatina Formation (Yerelina Subgroup). Unconformably overlain by Uratanna Formation.||
20148|Wilpena Group|68270|5|Briefly described|p683-684|Ediacaran|Ediacaran|Adelaide Rift Complex.|||Includes Bonney Sandstone.|Underlain by Umberatana Group.||
20148|Wilpena Group|68271|6|Mentioned|p693|Ediacaran|Ediacaran|Adelaide Rift Complex. Correlable to Billy Springs Formation.||||||
20148|Wilpena Group|68473|6|Mentioned|p531|||Adelaide Rift Complex.||||||
20148|Wilpena Group|68713|5|Briefly described|p19|||Spans the Elatina glaciation with interglacials in between.|||Includes the Billy Springs Formation.|||
20148|Wilpena Group|68735|6|Mentioned|p235 Fig.3|Neoproterozoic|Neoproterozoic|Arrowie Basin.||||||
20148|Wilpena Group|68822|6|Mentioned|p323|Ediacaran|Ediacaran|Deposition occurred around ca. 586 +/- 30 Ma||||||
20148|Wilpena Group|68993|6|Mentioned|p544 Fig.1|Neoproterozoic|Neoproterozoic|Arrowie Basin.||||||
20148|Wilpena Group|69019|5|Briefly described|p54-63, p144, p164.|Neoproterozoic|Neoproterozoic|Defined by Dalgarno and Johnson (in Thomson et al. 1964). Entirely Marinoan. Records two major transgressive-regressive cycles. Regional unconformity at the base.|||Includes Sandison and Pound Subgroups, Bunyeroo and Wonoka Formations.|||
20148|Wilpena Group|69255|6|Mentioned|p771|Neoproterozoic|Neoproterozoic|||||||
20148|Wilpena Group|69570|6|Mentioned|p421|||Pre-cambrian.||||||
20148|Wilpena Group|69666|6|Mentioned|p27 Fig.3|Neoproterozoic|Neoproterozoic|||||||
20148|Wilpena Group|69873|6|Mentioned|p82|||Adelaide Rift Complex. Included in diagram showing Cryogenian-Ediacaran stratigraphy and correlations with Tasmanian succession.||||||
20148|Wilpena Group|70021|6|Mentioned|p97|Neoproterozoic|Neoproterozoic|Northern Flinders Ranges, Adelaide Geosyncline.||||||
20148|Wilpena Group|70031|5|Briefly described|p245|Ediacaran|Ediacaran|Adelaide Geosyncline.|||Includes Pound Subgroup, Wonoka Formation, Bunyeroo Formation, ABC Range Quartzite, Brachina Formation and Nuccaleena Formation.|Underlain by Umberatana Group/Yerelina Subgroup.||
20148|Wilpena Group|70334|5|Briefly described|p2,19-20,30,36,55-56,81-82|Neoproterozoic|Neoproterozoic|Geological province: Gawler Craton. Of Adelaide Geosyncline and Stuart Shelf. Records post-glacial transgression followed by clastic progradation and a second transgressive-regressive cycle involving the cutting of submarine canyons (Preiss, 1987). Underwent erosion over the Cultana Inlier during fault reactivation of the Cultana Fault.|||Includes Wonoka Formation, Bunyeroo Formation and Sandison Subgroup.|||14-OCT-19
20148|Wilpena Group|70384|5|Briefly described|Map legend.|Ediacaran|Neoproterozoic|Adelaide Geosyncline.||Of Heysen Supergroup.|Includes Sandison, Pound Subgroups.|Unconformably overlies Umberatana Group.||23-JAN-19
20148|Wilpena Group|70406|6|Mentioned|p121 Fig 5||Neoproterozoic||||Includes Sandison Subgroup, Aruhna Subgroup, Depot Springs Subgroup.|Overlies Umberatana Group.||
20148|Wilpena Group|70407|5|Briefly described|p102 Fig 1, p103 Fig 2, p111, 112|Neoproterozoic|Neoproterozoic|Age: Ediacaran.||Of Heysen Supergroup.|Incudes Elatina Formation, Sandison Subgroup, Aruhna Subgroup, Depot Springs Subgroup, Pound Subgroup.|||
20148|Wilpena Group|70660|6|Mentioned|p34 fig 19e|||||||||
20148|Wilpena Group|70790|5|Briefly described|p257-258, p260 Fig.2, p268, p270|Neoproterozoic|Neoproterozoic|Adelaide Rift Complex. Is presented as Upper Wilpena Group and Lower Wilpena Group in Fig.2.|~620-525 Ma.||Nuccaleena Domolite; Brachina, Bunyeroo, Wonoka Formations; ABC Range Quartzite; Pound Subgroup.|||
20148|Wilpena Group|70838|6|Mentioned|p270|Neoproterozoic|Neoproterozoic|Deposition in a near- to off-shore rift setting.||||||
20148|Wilpena Group|71037|5|Briefly described|p22-23 Fig.2, p27 Fig.6, p27|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.|||Includes Tent Hill Formation.|Shown as younger than Umberatana Group and older than Sugarloaf Dam Sandstone.|White, red and purple shale, sandstone and quartzite; laminated; slumped  rey to reddish brown massive to cross-bedded quartzite;with silcrete skins.|
20148|Wilpena Group|71129|5|Briefly described|p17,117,128,138,184,208,225,227|Ediacaran|Ediacaran|Of southern Stuart Shelf and Adelaide Geosyncline. Records post-glacial transgression followed by clastic progradation during the Ediacaran Period (Preiss, 1987).|||Includes the Sandison Subgroup.|||13-NOV-19
20148|Wilpena Group|71130|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic||||Tent Hill Formation.|||
20148|Wilpena Group|71131|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic||||Tent Hill Formation.|||
20148|Wilpena Group|71236|6|Mentioned|p28|||||||||
20148|Wilpena Group|71237|14|Not recorded|p10, 19|||||||||
20148|Wilpena Group|71238|14|Not recorded|p1,2, 10|||||||||
20148|Wilpena Group|71241|4|Described|p12-15, p9-10|Marinoan|Marinoan|New name.||||||
20148|Wilpena Group|71242|14|Not recorded|p10|||||||||
20148|Wilpena Group|71250|6|Mentioned|p69-70|Ediacaran|Ediacaran|Central Flinders Ranges.|||Pound Subgroup; Nuccaleena, Brachina, Bunyeroo, Wonoka Formations; ABC Range Quartzite.||A succession of fluvial and marine sedimentary cycles.|
20148|Wilpena Group|71317|6|Mentioned|p15|Neoproterozoic|Neoproterozoic|Gawler Craton.||||||
20148|Wilpena Group|71322|5|Briefly described|p52 Fig.1|Neoproterozoic|Neoproterozoic||||||Quartzite, siltstone, shale; calcareous in part.|
20148|Wilpena Group|71712|6|Mentioned|p411||Neoproterozoic|||||||
20148|Wilpena Group|71895|5|Briefly described|p10, p11 fig 2|||Stuart Shelf.|||Includes the Nuccaleena Formation, Tregolana Shale Member, Corraberra Sandstone and Simmens Quartzite Member.|Unconformably overlies the Beda Basalt. Overlies the Umberatana Group.||
20148|Wilpena Group|72247|5|Briefly described|p43|Neoproterozoic|Neoproterozoic|Of Adelaide Geosyncline.|||Includes Arcoona Quartzite, Simmens Quartzite Member, Corraberra Sandstone Member, Woomera Shale, Tregolana Shale Member and Nuccaleena Formation.|Underlain by Umberatana Group.||
20148|Wilpena Group|72429|6|Mentioned|p952, p958, p972|Neoproterozoic|Marinoan|Mount Chambers Gorge, eastern Flinders Ranges[inferred].|||Includes the Brachina Formation.|Overlies the Umberatana Group.||
20148|Wilpena Group|72450|5|Briefly described|Brochure, Brochure map||||c. 600 ma||Includes the Seacliff Sandstone, Nuccaleena Formation, Brachina Formation, Port Stanvac Sandstone Member, ABC Range Quartzite, Bunyeroo Formation.|||
20148|Wilpena Group|72451|6|Mentioned|p2, p4, p5|||||||||09-JUN-20
20148|Wilpena Group|72489|6|Mentioned|p4 Fig.3|Ediacaran|Ediacaran|Adelaide Rift Complex. Only shown on p4 Fig.3. Simplified geological maps.||||||
20148|Wilpena Group|72613|6|Mentioned|p2 fig 1|Neoproterozoic|Neoproterozoic|Northern Flinders Ranges.||||||
20148|Wilpena Group|73092|6|Mentioned|p2|Cambrian|Neoproterozoic|||||||
20148|Wilpena Group|73100|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Subsurface. All the equivalent units are mapped as one unit.||||Equivalent to Punkerri Sandstone, Ungoolya Group (Rodda beds), Karlaya Limestone and Wright Hill beds.|Marine sandstone, grey indurated mudstone and limestone.|
20148|Wilpena Group|73109|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|The mapped unit is named Wilpena Group equivalents. Subsurface.||||Equivalent to Punkerri Sandstone, Ungoolya Group (Rodda beds), and Wright Hill beds.|Marine sandstone, grey indurated mudstone and limestone.|
20148|Wilpena Group|73111|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Subsurface. Presented as Wilpena Group equivalents.||||Equivalent to Punkerri Sandstone, Ungoolya Group (Rodda beds) and Wright Hill beds.|Marine sandstone, grey indurated mudstone and limestone.|
20148|Wilpena Group|73188|5|Briefly described|p305, p315-316, p341, p343, p351-353|Ediacaran|Ediacaran|Mount Lofty Ranges. Post-glacial. Deposited under mainly sag-phase conditions.|||Bunyeroo Formation, Sandison Subgroup, ABC Range Quartzite, Brachina Formation, Nuccaleena Formation, Seacliff Sandstone|||
20148|Wilpena Group|73222|5|Briefly described|p: 5-6, 8, 11-12, 16-17, 19-20, 24, 26|Ediacaran|Ediacaran|Adelaide Rift Complex. Marinoan. Thickness: 40 to 7,000 m. Deposited in an open marine, mixed siliciclastic and carbonate shelf with occasional nearshore and fluvial facies that correspond to topography created by the salt diapirs.||Heysen Supergroup|Pound Subgroup, Aruhna Subgroup, Sandison Subgroup, and units therein||Dolomite, limestone, calcareous sandstone, calcareous siltstone, siliceous siltstone, and shale.|
20148|Wilpena Group|73227|6|Mentioned|p25, p36||||||Tent Hill Formation, Tregolana Shale Member, Corraberra Sandstone Member, Simmens Quartzite Member, 'Arcoona Quartzite', 'Woomera Shale', Nuccaleena Formation|||
20148|Wilpena Group|73234|6|Mentioned|p5-6, p12, p20-21||||||Tent Hill Formation and units therein|||
20148|Wilpena Group|73236|5|Briefly described|p35-36, p38-40, p47|Ediacaran|Ediacaran|Marine sedimentary rocks.||Heysen Supergroup|Sandison Subgroup, ABC Range Quartzite, Brachina Formation, Nuccaleena Formation, Seacliff Sandstone, Wonoka Formation, Bonney Sandstone, Rawnsley Quartzite|[Unconformably] underlain by Reynella Siltstone Member (Elatina Formation, Yerelina Subgroup, Umberatana Group).||
20148|Wilpena Group|73251|6|Mentioned|p36|Neoproterozoic|Neoproterozoic|Coombalarnie Platform.||||Unconformably underlain by Umberatana Group.|Metasediments.|
20148|Wilpena Group|73262|6|Mentioned|p583|[Cryogenian?]|[Cryogenian?]|||Heysen Super Group|||Siltstone, quartzite, dolomite, marble, and sandy marble.|
20148|Wilpena Group|73264|6|Mentioned|p1386|||Adelaide Rift Complex.||||||
20148|Wilpena Group|74367|5|Briefly described|p3, p5-6, p7 Fig.6, p17, p19, p22|Ediacaran|Ediacaran|Post-glacial sequence, shoals upwards into predominantly sandstones.||Heysen Supergroup|Sandison Subgroup, Aruhna Subgroup, Depot Springs Subgroup, Pound Subgroup|||
20148|Wilpena Group|75063|6|Mentioned|p94 Fig.2|||Northern Flinders Ranges area.||||||
20152|Wilpoorinna Breccia Member|9862|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Of the Marree Formation. Basal slate-pebble breccia with boulders.||||||
20152|Wilpoorinna Breccia Member|23054|6|Mentioned|Fig5p22|Aptian|Aptian|||||||
20152|Wilpoorinna Breccia Member|23818|5|Briefly described|p141 Fig.65, p152|Early Cretaceous|Early Cretaceous|Geological Province: Great Artesian Basin. Of the Marree Formation. Underlying unit: Wilpena Group.||||||
20152|Wilpoorinna Breccia Member|24175|5|Briefly described|p23, p17 Fig. 3|Aptian|Aptian|Of the Bulldog Shale.  Elevated to formation status when parent unit Marree Formation was upgraded to Marree Subgroup.  See also p22.  Geological Province: Eromanga Basin.||||||
20152|Wilpoorinna Breccia Member|24321|5|Briefly described|Map legend|Aptian|Barremian|Parent: Bulldog Shale (of the Neales River Group).||||||
20152|Wilpoorinna Breccia Member|30804|6|Mentioned|Table 2|||||||||
20152|Wilpoorinna Breccia Member|30807|6|Mentioned|p102|||Suggested map symbol.||||||
20152|Wilpoorinna Breccia Member|33828|6|Mentioned|Table 1|||||||||
20152|Wilpoorinna Breccia Member|33939|5|Briefly described|p413|||Pelican Well Fm.||||||
20152|Wilpoorinna Breccia Member|34611|5|Briefly described|p153|||Lower Cretaceous. P152. See Fig.65.||||||
20152|Wilpoorinna Breccia Member|38068|6|Mentioned|p71|||||||||
20152|Wilpoorinna Breccia Member|39211|6|Mentioned|p26|||See also Fig.11||||||
20152|Wilpoorinna Breccia Member|40926|6|Mentioned|Table 2|||||||||
20152|Wilpoorinna Breccia Member|41085|6|Mentioned|p90|||See also Fig.1||||||
20152|Wilpoorinna Breccia Member|44133|4|Described|p105 Fig. 9.12, 117|Cretaceous|Cretaceous|Geological Province: Eromanga Basin. Of the Bulldog Shale (Marree Subgroup). Thickness: 5m.||||||
20152|Wilpoorinna Breccia Member|69019|5|Briefly described|p85 Fig.21, p95.|Aptian|Aptian|SW Eromanga Basin. Of Forbes et al. (1965) and Forbes (1966); type locality 4.5 km SE of Decoy Hill. Considered by White and Alley (this study) to be a very localised facies, not warranting Member status, and is now considered redundant.||Basal unit in Bulldog Shale.||Overlies Cadna-owie Formation.||
20152|Wilpoorinna Breccia Member|69023|6|Mentioned|p89 Fig.20|Aptian|Aptian|||||||
20155|Wilson Bluff Limestone|22587|6|Mentioned|p79 Fig.7|Late Eocene|Middle Eocene|||||||
20155|Wilson Bluff Limestone|22613|5|Briefly described|p21|Late Eocene|Middle Eocene|||||||
20155|Wilson Bluff Limestone|22614|5|Briefly described|map|Eocene|Eocene|||||||
20155|Wilson Bluff Limestone|22626|4|Described|437-439|Late Eocene|Middle Eocene|Geol province Eucla Basin. Max thickness 300 m||||||
20155|Wilson Bluff Limestone|22814|5|Briefly described|p258, fig2|Tertiary|Tertiary|||||||
20155|Wilson Bluff Limestone|23331|4|Described|1089|Late Eocene|Middle Eocene|||||||10-SEP-09
20155|Wilson Bluff Limestone|23488|5|Briefly described|p36, p38 Fig. 3|Middle Eocene|Middle Eocene|Geological Province: Eucla Basin.||||||
20155|Wilson Bluff Limestone|23533|6|Mentioned|p560|||See also p564 Fig 3.||||||
20155|Wilson Bluff Limestone|23584|6|Mentioned|p29|||Geological Province: Eucla Basin.||||||
20155|Wilson Bluff Limestone|23671|6|Mentioned|p1|||Disconformably overlies the Pidinga Formation.||||||
20155|Wilson Bluff Limestone|23768|5|Briefly described|p28 Fig. 5|Eocene|Eocene|Geological Province: Eucla Basin.  See also p39, p79.||||||
20155|Wilson Bluff Limestone|23818|4|Described|p174 Fig.84, p196, 198|Late Eocene|Middle Eocene|Geological Province: Eucla Basin. Max. thickness: 400 ft. Overlying unit: Nullarbor Limestone.||||||
20155|Wilson Bluff Limestone|23989|5|Briefly described|p54 Fig. 46|Late Eocene|Middle Eocene|Overlies Yilgarn Craton||||||04-NOV-10
20155|Wilson Bluff Limestone|24057|5|Briefly described|p97|Tertiary|Tertiary|Geological Basin: Eucla Basin.||||||
20155|Wilson Bluff Limestone|24094|4|Described|p272|Middle Eocene|Early Eocene|See also Wilson Bluff Limestone Formation. Li et al (1996) suggests the type section for Wilsons Bluff Limestone actually belongs to Abrakurrie Limestone. Geological Province: Eucla Basin||||||16-MAR-05
20155|Wilson Bluff Limestone|24201|5|Briefly described|p373 Fig. 2|Oligocene|Eocene|||||||
20155|Wilson Bluff Limestone|24338|5|Briefly described|p938 Fig. 2|Rupelian|Lutetian|Overlies the Pidinga Formation. Geological Province: Bight Basin.||||||
20155|Wilson Bluff Limestone|24347|5|Briefly described|p114|Late Eocene|Middle Eocene|Underlying unit: Hampton Sandstone.  Geological Province: Eucla Basin.||||||
20155|Wilson Bluff Limestone|24350|5|Briefly described|Fig. 4 Appdx|Oligocene|Eocene|Part of the Dugong Supersequence.||||||
20155|Wilson Bluff Limestone|24396|5|Briefly described|p222|Eocene|Eocene|Formerly contained the Paling Member (of Alley and Beecroft, 1993) however this member has now been raised to Paling Formation.  Overlies Gawler Craton.||||||04-NOV-10
20155|Wilson Bluff Limestone|24397|4|Described|p237-238|Eocene|Eocene|Formerly Wilson's Bluff Limestone (Singleton, 1954).  Geological Province: Eucla Basin.||||||
20155|Wilson Bluff Limestone|24443|5|Briefly described|Fig.7|Oligocene|Eocene|Overlies Piginda Formation. Geological Province: Bight Basin.||||||
20155|Wilson Bluff Limestone|24553|5|Briefly described|Figs. 7,8 and 10|Late Eocene|Middle Eocene|Along with Nullarbor Limestone, shown as equivalent to the Dugong Supersequence.||||||21-JAN-16
20155|Wilson Bluff Limestone|24557|5|Briefly described|p958, p959, p960 Fig.3|Late Eocene|Late Eocene|Offshore marine sediments: limestone and marl; biota dominated by bryozoans, with moderate foraminifera, echinoids, and locally abundant serpulids. Geological Province: Bremer Basin.||||||11-JAN-05
20155|Wilson Bluff Limestone|24606|5|Briefly described|p956|Late Eocene|Middle Eocene|Conformably overlies the Hampton Sandstone. Geological Province: Eucla Basin||||||
20155|Wilson Bluff Limestone|24617|6|Mentioned|p113, p115 Fig. 3|Eocene|Eocene|Geological Province: Eucla Basin.||||||
20155|Wilson Bluff Limestone|29591|5|Briefly described|p92|||||||||
20155|Wilson Bluff Limestone|29601|6|Mentioned|p82|||Upper Eocene||||||
20155|Wilson Bluff Limestone|29856|6|Mentioned|p37|||||||||
20155|Wilson Bluff Limestone|30012|4|Described|Table 1|||||||||
20155|Wilson Bluff Limestone|30230|6|Mentioned|p32|||Eocene age.||||||
20155|Wilson Bluff Limestone|30515|6|Mentioned|p69|||||||||
20155|Wilson Bluff Limestone|30563|4|Described|p12|||On Stratigraphic table||||||
20155|Wilson Bluff Limestone|30564|5|Briefly described|p4|||||||||
20155|Wilson Bluff Limestone|30807|6|Mentioned|p102|||Suggested map symbol||||||
20155|Wilson Bluff Limestone|30828|6|Mentioned|p113|||||||||
20155|Wilson Bluff Limestone|30917|6|Mentioned|p53|||||||||
20155|Wilson Bluff Limestone|30922|6|Mentioned|Map legend|Miocene|Miocene|||||||
20155|Wilson Bluff Limestone|30945|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
20155|Wilson Bluff Limestone|30975|6|Mentioned|Map legend|late Eocene|late Eocene|||||||
20155|Wilson Bluff Limestone|31049|6|Mentioned|p394|||||||||
20155|Wilson Bluff Limestone|31051|6|Mentioned|p.83.|||||||||
20155|Wilson Bluff Limestone|31053|6|Mentioned|p545|||||||||
20155|Wilson Bluff Limestone|31318|5|Briefly described|p166|||U. Eocene||||||
20155|Wilson Bluff Limestone|31562|5|Briefly described|p13|||||||||
20155|Wilson Bluff Limestone|31847|6|Mentioned|p49|||Correlation||||||
20155|Wilson Bluff Limestone|31850|4|Described|p33|||Summary of definition||||||
20155|Wilson Bluff Limestone|31902|4|Described|Table 1|||Fig.1||||||
20155|Wilson Bluff Limestone|31903|6|Mentioned|Map legend|Tertiary|Tertiary|Section only||||||
20155|Wilson Bluff Limestone|31904|4|Described|p7|||See Table 1. Refers previous authors.||||||
20155|Wilson Bluff Limestone|31906|4|Described|p7|||See Table 1. Refers previous authors.||||||
20155|Wilson Bluff Limestone|31907|3|Fully described|p7|||See also Table 1, Fig.1||||||
20155|Wilson Bluff Limestone|31908|4|Described|Table 1|||U.-M. Eocene||||||
20155|Wilson Bluff Limestone|31909|3|Fully described|p7|||||||||
20155|Wilson Bluff Limestone|31913|4|Described|p10|||Table 1||||||
20155|Wilson Bluff Limestone|31915|6|Mentioned|Map legend|Eocene|Eocene|||||||
20155|Wilson Bluff Limestone|31923|6|Mentioned|p18|||||||||
20155|Wilson Bluff Limestone|32117|6|Mentioned|Fig.2|||||||||
20155|Wilson Bluff Limestone|32120|6|Mentioned|p276|||Eocene fauna||||||
20155|Wilson Bluff Limestone|32552|2|Defined|p10|late Eocene|middle Eocene|Mid.-U.Eocene. See also P27, 37, 53, 54 etc.M - U||||||
20155|Wilson Bluff Limestone|32648|6|Mentioned|p32|||U.Eocene||||||
20155|Wilson Bluff Limestone|32750|6|Mentioned|p304|||Stratigraphy||||||
20155|Wilson Bluff Limestone|33586|4|Described|Table 1|||See also P14.||||||
20155|Wilson Bluff Limestone|33589|4|Described|p11|||U. Eocene.||||||
20155|Wilson Bluff Limestone|33595|6|Mentioned|p6|||||||||
20155|Wilson Bluff Limestone|34180|6|Mentioned|p229|||Tertiary||||||
20155|Wilson Bluff Limestone|34192|6|Mentioned|Map legend|Oligocene|Eocene|Lower Miocene - Eocene||||||
20155|Wilson Bluff Limestone|34194|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
20155|Wilson Bluff Limestone|34232|6|Mentioned|p76|||Cavities.||||||
20155|Wilson Bluff Limestone|34287|6|Mentioned|p200|||||||||
20155|Wilson Bluff Limestone|34308|4|Described|p196|||M.- U.Eocene. Cor. chart Fig.84||||||
20155|Wilson Bluff Limestone|34344|6|Mentioned|p3|||Middle Eocene.||||||
20155|Wilson Bluff Limestone|34615|6|Mentioned|p10|||||||||
20155|Wilson Bluff Limestone|34742|6|Mentioned|Map legend|late Eocene|late Eocene|||||||
20155|Wilson Bluff Limestone|34759|6|Mentioned|p60|||||||||
20155|Wilson Bluff Limestone|35051|6|Mentioned|p204|||||||||
20155|Wilson Bluff Limestone|35097|6|Mentioned|p16|||||||||
20155|Wilson Bluff Limestone|35496|4|Described|Table 1|||Also on p21.||||||13-SEP-18
20155|Wilson Bluff Limestone|35772|6|Mentioned|Table 1|||See also p11.||||||13-SEP-18
20155|Wilson Bluff Limestone|36200|6|Mentioned|Table 1|||||||||
20155|Wilson Bluff Limestone|36257|6|Mentioned|Table 2.1|||||||||
20155|Wilson Bluff Limestone|36890|3|Fully described|p413|||Formerly Wilsons Bluff Limestone||||||
20155|Wilson Bluff Limestone|36915|6|Mentioned|Fig.7|||||||||
20155|Wilson Bluff Limestone|37852|6|Mentioned|p5|||||||||
20155|Wilson Bluff Limestone|38068|6|Mentioned|Fig.7|||||||||
20155|Wilson Bluff Limestone|38553|6|Mentioned|p41|||||||||
20155|Wilson Bluff Limestone|38602|6|Mentioned|p2|||||||||
20155|Wilson Bluff Limestone|38773|6|Mentioned|p46|||||||||
20155|Wilson Bluff Limestone|39173|6|Mentioned|p325|||||||||
20155|Wilson Bluff Limestone|39923|6|Mentioned|p354|||||||||
20155|Wilson Bluff Limestone|40003|5|Briefly described|Table 14|||See also Fig.16 and P54||||||
20155|Wilson Bluff Limestone|40298|6|Mentioned|p433|||||||||
20155|Wilson Bluff Limestone|40410|6|Mentioned|p4|||||||||
20155|Wilson Bluff Limestone|40421|6|Mentioned|p60|||||||||
20155|Wilson Bluff Limestone|40429|6|Mentioned|p26|||||||||
20155|Wilson Bluff Limestone|40992|6|Mentioned|Fig.23|||||||||
20155|Wilson Bluff Limestone|41043|6|Mentioned|p87|||||||||
20155|Wilson Bluff Limestone|41076|6|Mentioned|p70|||||||||
20155|Wilson Bluff Limestone|41517|6|Mentioned|p139|||||||||
20155|Wilson Bluff Limestone|41626|6|Mentioned|p48|||||||||
20155|Wilson Bluff Limestone|42086|5|Briefly described|Fig.2 P4|||||||||
20155|Wilson Bluff Limestone|42108|4|Described|p321|||See also Fig.1||||||
20155|Wilson Bluff Limestone|42335|4|Described|p325|||||||||
20155|Wilson Bluff Limestone|42356|5|Briefly described|Fig.15 P119|late Eocene|middle Eocene|See also Microfiche 7 p15, Fig.4, Fig.9, 10, 12, 13.||||||
20155|Wilson Bluff Limestone|42428|5|Briefly described|p1006|||||||||
20155|Wilson Bluff Limestone|42734|5|Briefly described|map legend|Tertiary||||||||
20155|Wilson Bluff Limestone|42816|5|Briefly described|p23|||||||||
20155|Wilson Bluff Limestone|42862|5|Briefly described|p8|||||||||
20155|Wilson Bluff Limestone|42959|5|Briefly described|p58 Fig.3|||||||||
20155|Wilson Bluff Limestone|43026|6|Mentioned|p589|||||||||
20155|Wilson Bluff Limestone|43040|5|Briefly described|Fig.2,p861|||||||||
20155|Wilson Bluff Limestone|43049|5|Briefly described|p23|||||||||
20155|Wilson Bluff Limestone|43065|5|Briefly described|Fig.5,p92|Late Eocene|Middle Eocene|||||||
20155|Wilson Bluff Limestone|43498|6|Mentioned|8||Late Eocene|||||||
20155|Wilson Bluff Limestone|43658|6|Mentioned|p5||Eocene|||||||
20155|Wilson Bluff Limestone|43672|5|Briefly described|p330|||||||||
20155|Wilson Bluff Limestone|43813|6|Mentioned|p133|||||||||
20155|Wilson Bluff Limestone|43814|6|Mentioned|Fig.3,p115|||||||||
20155|Wilson Bluff Limestone|44133|4|Described|p182|Early Oligocene|Middle Eocene|Geological Province: Eucla Basin. Conformably overlies: Pidinga Formation and Hampton Sandstone. Thickness: ~300m. Intertongues and underlies Toolinna Limestone. Underlies Abrakurrie and Nullarbor Limestones.||||||11-JUL-13
20155|Wilson Bluff Limestone|44145|4|Described|p551 Tbl 4-27, p555-6, fig 4-194,|Late Eocene|Middle Eocene|Eucla Basin. Thickness up to 300m known. Rich and varied fauna.||||Disconformably overlies Madura Formation. Overlies and grades laterally into Hampton Sandstone. Upper part grades laterally into Toolinna Limestone. Unconformably overlain by Abracurrie Limestone.|Chalky bryozoan calcarenite packstone with chert nodules. Basal glauconitic marl in places.|
20155|Wilson Bluff Limestone|44412|14|Not recorded|map legend||Eocene|Middle to Upper Eocene.||||||
20155|Wilson Bluff Limestone|44695|5|Briefly described|Map Legend|Eocene|Eocene|(Middle-Late Eocene)||||||
20155|Wilson Bluff Limestone|44864|5|Briefly described|Map Legend||Miocene|||||||
20155|Wilson Bluff Limestone|45149|4|Described|p62|||See also p60.||||||13-SEP-18
20155|Wilson Bluff Limestone|45168|6|Mentioned|Table 1 P6|||||||||
20155|Wilson Bluff Limestone|47054|6|Mentioned|p490|||||||||
20155|Wilson Bluff Limestone|61155|5|Briefly described|p3, p17|Late Eocene|Middle Eocene|Includes bryozoan clacarenites. Overlies and interfingers with Hampton Sandstone; overlain by and interfingers with Toolinna Limestone. Age: 44-38.5Ma. Max. thickness: 300m. Geological Province: Eucla Basin and the Great Australian Bight.||||||
20155|Wilson Bluff Limestone|61197|5|Briefly described|p473, p475, p478 Fig.4, p488|Late Eocene|Middle Eocene|Eucla Basin. Marine deep-shelf deposits. 0-40m thick.|||||Chalky, bryozoan calcarenite; common chert nodules; minor glauconite.|
20155|Wilson Bluff Limestone|61517|5|Briefly described|p309|Eocene|Eocene|Unconformably overlain by Roe Calcarenite. Geological Province: Eucla Basin.||||||
20155|Wilson Bluff Limestone|61544|6|Mentioned|p367 Fig.3. |Eocene|Eocene|||||Overlies Pidinga Formation.||
20155|Wilson Bluff Limestone|61630|6|Mentioned|p555 Fig. 3|Oligocene|Eocene|Geological Province: Eyre Sub-basin, Bright and Duntroon Basins. Marine.||||||07-APR-09
20155|Wilson Bluff Limestone|61856|5|Briefly described|p300 Fig.2, p304, p311, p314-317 |Eocene|Eocene|Thickness: up to 300m.||||Conformably overlies Hampton Sandstone.|Thick marine limestone; sandy and glauconitic in the lower part.|23-JAN-15
20155|Wilson Bluff Limestone|62369|5|Briefly described|p409, p410 Fig.4|Late Eocene|Middle Eocene|White, muddy, burrowed unit, rich in bryozoans and planktonic foraminifers. Overlies Hampton Sandstone. Thickness: ~300m. Geological Province: Eucla Basin.||||||04-NOV-10
20155|Wilson Bluff Limestone|62640|5|Briefly described|p65, pp67-77.       |Late Eocene|Middle Eocene|Oldest and thickest limestone of the Eucla Basin; up to 300m thick. High porosity, low permeability.|c.42 - c.37 Ma.|||Overlies Madura Formation. Intertongues with the Toolinna Limestone in the southwest of the Eucla Basin. Is overlain by Abrakurrie Limestone.|Predominantly sand-sized fragments of calcareous skeletons in a very fine-grained calcite matrix.|
20155|Wilson Bluff Limestone|64646|6|Mentioned|p23 Fig. 3, p24 Fig. 4|Oligocene|Late Eocene|Geological Province: Eucla Basin.||||||08-FEB-10
20155|Wilson Bluff Limestone|65891|6|Mentioned|p221 Fig.5. |Paleogene|Paleogene|East Eucla Basin. Age shown as Lutetian to Priabonian.||||||
20155|Wilson Bluff Limestone|65942|2|Defined|p77-78||Miocene|||Of Eucla Group.||||
20155|Wilson Bluff Limestone|66131|6|Mentioned|p242 Fig.2|Eocene|Eocene|Middle to Late Eocene in age (from p.242 Fig.2 - stratigraphic correlation chart).||||||
20155|Wilson Bluff Limestone|67117|5|Briefly described|Map legend.|Miocene|Eocene|Shown under general heading of 'Eocene - Miocene'.|||||White to grey wackestone; skeletal mudstone, rudstone and minor packstone; locally laminations and scour channels, infilled with coarser material.|03-MAY-13
20155|Wilson Bluff Limestone|67462|5|Briefly described|Map legend.|Eocene|Eocene|Bunda Plateau, Eucla Basin.||||||
20155|Wilson Bluff Limestone|67789|5|Briefly described|p34-35, 39-40, 45-46|Eocene|Eocene|Eucla Basin. Up to 300m thick. Contains the best developed deep caves in the Nullarbor Plain.||Eucla Group.||Is overlain by Abrakurrie Limestone.|A soft, poorly lithified, muddy to chalky bryozoan-rich cool-water carbonate.|
20155|Wilson Bluff Limestone|68715|6|Mentioned|p30 Fig.5|Priabonian|Lutetian|Bunda Plateau, Eucla Basin.||||||23-JAN-15
20155|Wilson Bluff Limestone|69004|5|Briefly described|p19, p34|Upper Eocene|Middle Eocene|Eucla Basin. Informally subdivided into an upper and lower part.|||||Carbonates including limestone.|
20155|Wilson Bluff Limestone|69598|5|Briefly described|p2, p9, p11 Tb.1, p29 Tb.4|||Eucla Basin. Up to 300m thick. Potential carbon dioxide storage reservoir.|||||Fine-grained to chalky limestone that is commonly rich in bryozoans and echinoids.|
20155|Wilson Bluff Limestone|69648|4|Described|p4, p22-24, map legend|Eocene|Eocene|Eucla Basin. Temperate water, bryozoan limestones form foundation of a carbonate platform. First recognised by Tate (1879), who referred to it as the 'white polyzoal limestone'. Forms lower white band of cliffs that front the Great Australian Bight. Was deposited on a very broad (i.e. ~1000 km wide) and gently inclined platform, or a ramp where the higher energy facies predominate near the shore. The generally muddy nature of sediments indicate deposition mostly below fairweather wavebase. Age: Middle to Late Eocene (modified to early Late Eocene by Alley and Beecroft, 1993); significantly eroded during Oligocene to Early Miocene. Thickness: >50 m in SW OOLDEA and increases toward platform margin to ~300 m.||Eucla Group|Paling Member|Conformably overlies, and interfingers with, Pidinga Formation and Hampton Sandstone.|Marine platform bioclastic carbonates; dominantly muddy or micritic, bryozoan limestone; skeletal mudstone, wackestone (dominant), packstone and grainstone, and rudstone textures; lower/basal part can be glauconitic.|
20155|Wilson Bluff Limestone|69649|6|Mentioned|p31,|Eocene|Eocene|Eucla Basin.||||||
20155|Wilson Bluff Limestone|70397|5|Briefly described|p1-3|Late Eocene|Middle Eocene|Eucla Basin. Depositional environment: cool-temperate, open-marine shelf.||Unit of Eucla Group.||Unconformabyl overlain by Abrakurrie Limestone. Underlain by Hampton Sandstone.|Fine- to medium-grained bryozoan and planktonic foraminifera facies.|29-JUL-19
20155|Wilson Bluff Limestone|70722|5|Briefly described|p227-228|Eocene|Eocene|Of St. Vincent Basin. Lithologically different from Kangaroo Island late Eocene limestones, and areal distribution confirms a strong shelf partitioning, inboard biosiliceous and outboard carbonate (Gammon et al., 2003).|||||Fine-grained bryozoan-rich chalky limestones.|
20155|Wilson Bluff Limestone|70771|4|Described|p3, p7-p8, p27, p53-p58, p60-p61|Late Eocene|Middle Eocene|Eucla Platform, Eucla Basin. Commonly fossiliferous including abundant bryozoans, echinoids, bivalves, brachiopods and foraminifers. Extends to the inner margin of the Eucla Platform attaining a maximum thickness of approximately 300m. Interpreted to have been deposited on a cool to temperate continental shelf in water depths of 90-120m. [The author assigns this unit to the Eucla Group however this term is obsolete].||Eucla Group||Overlies the Hampton Sandstone. Disconformably overlain by the Abrakurrie Limestone and the Roe Calcarenite.|White, poorly-sorted chalky and fossiliferous limestone.|
20155|Wilson Bluff Limestone|70778|5|Briefly described|p4, p10|||Intersected in Nundroo 3 DDH.|||||Calcareous mudstone and glauconite.|
20155|Wilson Bluff Limestone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||greywacke|
20155|Wilson Bluff Limestone|71361|4|Described|p5, p12, p15-p18, p23, p120|Late Eocene|Middle Eocene|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 to temperate deep shelf with water up to 300m deep. This unit contains abundant bryozoan and planktonic foraminifera fossils.||Eucla Group||Overlies the Hampton Sandstone. Unconformably overlain by the Abrakurrie Limestone and the Nullarbor Limestone.|Fine-grained bryozoan limestone, wackestone, packstone, chalky mudstones and grainstones.|
20155|Wilson Bluff Limestone|71789|14|Not recorded|p101|||Equivalent to Pallinup Siltstone.||||||
20155|Wilson Bluff Limestone|72344|5|Briefly described|p5, p16, p49, p61|||Eucla Basin. <150m thick east of the Coompana Block, increasing westwards to up to 300m thick in WA. Interpreted to have been deposited in a marine transgression on a drowned carbonate platform. See also p84, p96, p160, p169.||||Overlies the Hampton Sandstone. Overlain by the Abrakurrie Limestone.|Wackestone, white to grey, skeletal mudstone; rudstone and minor packstone. Locally laminations and scour channels infilled with coarser material.|
20155|Wilson Bluff Limestone|72465|5|Briefly described|p9, 14-15, 17|Tertiary|Tertiary|Eucla Basin, Coompana Province. <150m thick E of the Coompana Block, increasing westwards to 300m thick in WA. Forms the whitish cross-bedded and parallel-bedded unit in the lower Bunda Cliffs.||||Overlies Hampton Sandstone. Is overlain by Abrakurrie Limestone.|Wackestone, white to grey; skeletal mudstone; rudestone and minor packstone. Local laminations and minor scour channels, infilled with coarser material.|
20155|Wilson Bluff Limestone|72466|5|Briefly described|p9, 14-15, 17|Tertiary|Tertiary|Benbow et al. (1995). Eucla Basin, Coompana Province. <150m thick east of the Coompana Block, thickening westwards to 300m thick in WA. Deposited during marine transgressions on a drowned carbonate platform. Forms whitish cross-bedded and parallel-bedded unit in lower parts of the Bunda Cliffs. Also appears as Wilson's Bluff Limestone on p14 and as Wilsons Bluff limestone on p15.||||Overlies Hampton Sandstone and Pidinga Formation. Is overlain by Abrakurrie Limestone.|Wackestone, white to grey, skeletal mudstone, rudstone and minor packstone. Locally laminations and scour channels, infilled with coarser material.|
20155|Wilson Bluff Limestone|72467|5|Briefly described|p9, 14-15, 17|Tertiary|Tertiary|Eucla Basin, Coompana Province. <150m thick E of the Coompana Block, increasing westwards to 300m thick in WA. Forms the whitish cross-bedded and parallel-bedded unit in the lower Bunda Cliffs. Also appears as Wilson's Bluff Limestone (p14) and Wilsons Bluff Limestone (p15).||||Overlies Hampton Sandstone. Is overlain by Abrakurrie Limestone.|Wackestone, white to grey; skeletal mudstone; rudestone and minor packstone. Local laminations and minor scour channels, infilled with coarser material.|
20155|Wilson Bluff Limestone|72468|5|Briefly described|p9, p14-15, p17|||[Also written as Wilson's Bluff Limestone]. Eucla Basin. Less than 150 m thick in the east, thickening to c. 300 m in the west. Deposited during marine transgression on a drowned carbonate platform. Forms the whitish cross-bedded and parallel-bedded unit in the lower parts of the Bunda Cliffs. Hosts an unconfined aquifer.||||Underlain by Hampton Sandstone. Overlain by Abrakurrie Limestone.|Wackestone, white to grey; skeletal mudstone; rudstone and minor packstone. Locally laminations and scour channels, infilled with coarser material.|
20155|Wilson Bluff Limestone|72469|5|Briefly described|p9, p14-15, p17|||[Also written as Wilson's Bluff Limestone]. Eucla Basin. Less than 150 m thick in the east, thickening to c. 300 m in the west. Deposited during marine transgression on a drowned carbonate platform. Forms the whitish cross-bedded and parallel-bedded unit in the lower parts of the Bunda Cliffs. Hosts an unconfined aquifer.||||Underlain by Hampton Sandstone. Overlain by Abrakurrie Limestone.|Wackestone, white to grey; skeletal mudstone; rudstone and minor packstone. Locally laminations and scour channels, infilled with coarser material.|
20155|Wilson Bluff Limestone|72470|5|Briefly described|p9, p14-15, p18|||[Also written as Wilson's Bluff Limestone]. Eucla Basin. Less than 150 m thick in the east, thickening to c. 300 m in the west. Deposited during marine transgression on a drowned carbonate platform. Forms the whitish cross-bedded and parallel-bedded unit in the lower parts of the Bunda Cliffs. Hosts an unconfined aquifer.||||Underlain by Hampton Sandstone. Overlain by Abrakurrie Limestone.|Wackestone, white to grey; skeletal mudstone; rudstone and minor packstone. Locally laminations and scour channels, infilled with coarser material.|
20155|Wilson Bluff Limestone|72471|5|Briefly described|p9, p15, p17|||Eucla Basin. Less than 150 m thick in the east, thickening to c. 300 m in the west. Deposited during marine transgression on a drowned carbonate platform. Forms the whitish cross-bedded and parallel-bedded unit in the lower parts of the Bunda Cliffs.||||Underlain by Hampton Sandstone. Overlain by Abrakurrie Limestone.|Wackestone, white to grey; skeletal mudstone; rudstone and minor packstone. Locally laminations and scour channels, infilled with coarser material.|
20155|Wilson Bluff Limestone|72472|5|Briefly described|p9, p14-15|||[Also written as Wilson's Bluff Limestone]. Eucla Basin. Less than 150 m thick in the east, thickening to c. 300 m in the west. Deposited during marine transgression on a drowned carbonate platform. Forms the whitish cross-bedded and parallel-bedded unit in the lower parts of the Bunda Cliffs. Hosts an unconfined aquifer.||||Underlain by Hampton Sandstone. Overlain by Abrakurrie Limestone.|Wackestone, white to grey; skeletal mudstone; rudstone and minor packstone. Locally laminations and scour channels, infilled with coarser material.|
20155|Wilson Bluff Limestone|73084|5|Briefly described|p16-17|Eocene|Eocene|Eucla Basin.||||Underlain by Hampton Sandstone. Overlain by Nullarbor Limestone.|Chalky, fossiliferous limestone.|
20155|Wilson Bluff Limestone|73112|5|Briefly described|Map legend.|Eocene|Eocene||||||White bryozoal chalk with flints.|
20155|Wilson Bluff Limestone|73641|5|Briefly described|p5|Eocene|Eocene|Eucla Basin. 150 to ~300m thick. Deposited during a marine transgression on a drowned carbonate platform.||||Overlies Hampton Sandstone. Is overlain by Abrakurrie Limestone.|White to grey skeletal mudstone, rudstone and minor packstone. Local laminations and scour channels infilled with coarser material.|
20181|Wiltabbie Volcanics|24472|5|Briefly described|p5 Tb.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Harris Greenstone Domain, Gawler Craton. Age: ~1590Ma||||||
20181|Wiltabbie Volcanics|42469|6|Mentioned|p19|||on Tarcoola sheet SH53-10.||||||
20181|Wiltabbie Volcanics|42546|5|Briefly described|Map legend|Mesoproterozoic||||||||
20181|Wiltabbie Volcanics|42736|5|Briefly described|map legend|Mesoproterozoic||||||||
20181|Wiltabbie Volcanics|43052|5|Briefly described|p117|||||||||
20181|Wiltabbie Volcanics|44935|5|Briefly described|Map Legend||Proterozoic|||||||
20181|Wiltabbie Volcanics|67058|5|Briefly described|p479 Fig. 3|Mesoproterozoic|Mesoproterozoic|Gawler Craton|||||Rhyolite, dacite, andesite, basalt, dolerite, dykes|19-APR-12
20181|Wiltabbie Volcanics|68128|5|Briefly described|p53|||Gawler Craton.|||||Rhyolite, dacite, andesite and basalt.|01-FEB-23
20181|Wiltabbie Volcanics|68131|6|Mentioned|p77|Mesoproterozoic|Mesoproterozoic|||||||
20181|Wiltabbie Volcanics|72090|6|Mentioned|p12|||Gawler Craton.|||||Rhyolite to basalt dykes.|
20188|Wilyerpa Formation|22510|5|Briefly described|p38, Table1p37|||Of the Yudnamutana Subgroup.  Age: Sturtian.||||||13-FEB-08
20188|Wilyerpa Formation|22631|6|Mentioned|p178|||Age: Sturtian.||||||
20188|Wilyerpa Formation|22926|6|Mentioned|39 fig 2|Neoproterozoic|Neoproterozoic|||||||
20188|Wilyerpa Formation|23250|5|Briefly described|p1124 Fig.2||Cryogenian|of Umberatana Group. On diagram as Wilyerpa - assumed to be Wilyerpa Formation. Correlate of Areyonga Formation.||||||
20188|Wilyerpa Formation|23351|5|Briefly described|283|Neoproterozoic|Neoproterozoic|||||||
20188|Wilyerpa Formation|23477|5|Briefly described|p49 Fig 3|Neoproterozoic|Neoproterozoic|Of Yudnamutana Subgroup. Geological Province: Curnamona Province.||||||
20188|Wilyerpa Formation|23818|5|Briefly described|p64 Fig.22|Neoproterozoic|Neoproterozoic|Of the Yudnamutana Sub-Group.||||||
20188|Wilyerpa Formation|23913|4|Described|p110 Fig. 2|Adelaidean|Adelaidean|Geological Province: Central Flinders Zone. Of the Umberatana Group. Underlying Unit: Holowilena Ironstone. Overlying Unit: Tapley Hill Formation.||||||13-FEB-08
20188|Wilyerpa Formation|24175|3|Fully described|p12|Neoproterozoic|Neoproterozoic|Of Umberatana Group. May unconformably overlie Bolla Bollana Tillite.  Max. thickness: 584m.||||||13-FEB-08
20188|Wilyerpa Formation|24321|5|Briefly described|Map legend|Adelaidean|Adelaidean|Parent: Umberatana Group.||||||13-FEB-08
20188|Wilyerpa Formation|24476|4|Described|p547 Fig. 4|Adelaidean|Adelaidean|Overlain by the Tapley Hill Formation. Geological Province: Adelaide fold belt.||||||25-JAN-08
20188|Wilyerpa Formation|24584|5|Briefly described|p14 Fig. 2|Neoproterozoic|Neoproterozoic|Siltstone, sandstone.||||||
20188|Wilyerpa Formation|29780|6|Mentioned|p32|||||||||
20188|Wilyerpa Formation|30178|6|Mentioned|p20|||||||||
20188|Wilyerpa Formation|30801|6|Mentioned|p5|||Preferred name to Wilyerpa Quartzite. Table P5-6||||||
20188|Wilyerpa Formation|30802|4|Described|p12|||Sturtian age.||||||
20188|Wilyerpa Formation|30807|6|Mentioned|p103|||Suggested map symbol||||||
20188|Wilyerpa Formation|30810|6|Mentioned|p2|||||||||
20188|Wilyerpa Formation|32510|6|Mentioned|Table 1|||||||||
20188|Wilyerpa Formation|32724|6|Mentioned|Fig.1|||Sturtian. Correlation||||||
20188|Wilyerpa Formation|33474|6|Mentioned|Fig.2|||||||||
20188|Wilyerpa Formation|34267|6|Mentioned|p105|||||||||
20188|Wilyerpa Formation|34535|6|Mentioned|Fig.22|||||||||
20188|Wilyerpa Formation|35200|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
20188|Wilyerpa Formation|35232|6|Mentioned|p6|||See also Table 1.||||||
20188|Wilyerpa Formation|35255|6|Mentioned|p13|||||||||
20188|Wilyerpa Formation|35904|6|Mentioned|p9|||||||||
20188|Wilyerpa Formation|36838|6|Mentioned|p57|||||||||
20188|Wilyerpa Formation|37238|6|Mentioned|p366|||||||||
20188|Wilyerpa Formation|37461|6|Mentioned|Table 5.I|||||||||
20188|Wilyerpa Formation|37932|4|Described|p542|||See also P539.||||||
20188|Wilyerpa Formation|38157|6|Mentioned|Table IV|||||||||
20188|Wilyerpa Formation|39344|6|Mentioned|Map legend|Precambrian|Precambrian|Sturtian||||||
20188|Wilyerpa Formation|39348|6|Mentioned|Map legend|Precambrian|Precambrian|Sturtian||||||
20188|Wilyerpa Formation|40225|6|Mentioned|Map sheet|||||||||
20188|Wilyerpa Formation|40294|3|Fully described|p43|||See also P12||||||
20188|Wilyerpa Formation|40914|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
20188|Wilyerpa Formation|41405|3|Fully described|p156|||||||||
20188|Wilyerpa Formation|41496|5|Briefly described|Fig.1|||||||||
20188|Wilyerpa Formation|41526|6|Mentioned|p8|||||||||
20188|Wilyerpa Formation|41647|6|Mentioned|p843|||||||||
20188|Wilyerpa Formation|42090|5|Briefly described|p25|||||||||
20188|Wilyerpa Formation|42098|5|Briefly described|p53|||||||||
20188|Wilyerpa Formation|42101|6|Mentioned|p84|||||||||
20188|Wilyerpa Formation|42238|5|Briefly described|p73|||||||||
20188|Wilyerpa Formation|42239|6|Mentioned|Fig.2 P151|||||||||
20188|Wilyerpa Formation|42272|6|Mentioned|Fig.2 P400|||||||||
20188|Wilyerpa Formation|42720|5|Briefly described|map legend|Sturtian||||||||
20188|Wilyerpa Formation|42813|4|Described|p20|||Of Umberatana Group.||||||13-FEB-08
20188|Wilyerpa Formation|42882|4|Described|p5, Fig.4 p7|||Of Umberatana Group.||||||13-FEB-08
20188|Wilyerpa Formation|43052|5|Briefly described|p186,Table 6.1|||||||||
20188|Wilyerpa Formation|43742|6|Mentioned|Fig.2,p39||Neoproterozoic|||||||
20188|Wilyerpa Formation|43845|5|Briefly described|Fig3 p43, 41,42||Neoproterozoic|In Umberatana Group.||||||12-JUL-16
20188|Wilyerpa Formation|46865|6|Mentioned|p50|||||||||
20188|Wilyerpa Formation|60718|5|Briefly described|p49 Fig. 2, p53|Adelaidean|Adelaidean|Includes pebbly and quartzitic diamictite. Geological Province: Adelaide Geosyncline. See also p51 Fig. 3, p52.||Of Yudnamutana Subgroup (Umberatana Group).||Unconformably underlies Serle Conglomerate.||15-APR-11
20188|Wilyerpa Formation|60959|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Of the Yudnamutana Subgroup. Green siltstone. Includes glacial dropstones, medium to coarse grained sandstone, glacial conglomerate.||||||
20188|Wilyerpa Formation|61732|5|Briefly described|p28 Fig. 13|Sturtian|Sturtian|Of the Yudnamutana Subgroup (Umberatana Group). Includes the Warcowie Dolomite Member. Geological Province: Adelaide Rift Complex.||||||07-FEB-11
20188|Wilyerpa Formation|62085|6|Mentioned|p20 fig 5|Cryogenian|Cryogenian|||Umberatana Group||Overlies Holowilena Ironstone. Is overlain by Tapley Hill Formation.||
20188|Wilyerpa Formation|62592|5|Briefly described|p50 Table 5.1, p58.|Sturtian|Sturtian|Adelaide Geosyncline. Up to 3,550 m thick in Bibliando Dome, Flinders Ranges.||Unit in Yudnamutana Subgroup.||Unconformably overlies Benda Siltstone.|Siltstone, sandstone, minor conglomerate and diamictite, basal dolomite.|
20188|Wilyerpa Formation|62724|5|Briefly described|p16, p17 Fig. 4|Sturtian|Sturtian|Of the Yudnamutana Subgp (Umberatana Gp). Very thick siltstone-dominated succession. Overlies Holowilena Ironstone (in Flinders Ranges); unconformable over Benda Siltstone. Geological Province: Olary Domain/Curnamona Province.||||||07-FEB-11
20188|Wilyerpa Formation|62903|5|Briefly described|p729, p730 Fig.1, p731|||Adelaide Rift Complex.||Yudnamutana Subgroup||||
20188|Wilyerpa Formation|62993|5|Briefly described|p31|Neoproterozoic|Neoproterozoic||||||Diamictites.|
20188|Wilyerpa Formation|63102|5|Briefly described|p8,46|Neoproterozoic|Neoproterozoic|Geological province: Curnamona Province.||Unit of Yudnamutana Group.||Underlain unconformably by Benda Siltstone.|Siltstone, sandstone, diamictite.|
20188|Wilyerpa Formation|63458|6|Mentioned|p897 Fig.19. |Cryogenian|Cryogenian|||Unit in Yudnamutana Subgroup.||||
20188|Wilyerpa Formation|64797|5|Briefly described|p158-159, p162 Fig.9, p163 Tb.5. |||See also p168 Tb.11. S-isotope data.||||||
20188|Wilyerpa Formation|64801|6|Mentioned|p112|Neoproterozoic|Neoproterozoic|||||||
20188|Wilyerpa Formation|65892|5|Briefly described|p33 Fig.18.|Cryogenian|Cryogenian|||Unit in Umberatana Group.||Overlies Holowilena Ironstone. Is overlain by Tapley Hill Formation.||
20188|Wilyerpa Formation|65925|5|Briefly described|Appendix 2.||||||||Siltstone, green. Lower third is fine grained, includes glacial dropstones; middle unit is medium to coarse sandstone; upper unit is siltstone with minor sandstone. Minor diamictite, sandy and pebbly dolomite.|
20188|Wilyerpa Formation|66464|6|Mentioned|p168 Fig.2|Cryogenian|Cryogenian|SHRIMP U-Pb zircon age of 659.7 +/- 5.3 Ma (Fanning, 2006) from a tuffaceous horizon just above the Sturtian diamictite.||||||
20188|Wilyerpa Formation|66884|6|Mentioned|p44|||||||Overlies unnamed upper member of Myrtle Springs Formation.||
20188|Wilyerpa Formation|67030|5|Briefly described|p408, p409 Fig. 2|Cryogenian|Cryogenian|SE Flinders Ranges. No supporting information in relation to age|~659 Ma|||Underlies the Tapley Hill Formation; equivalent to the Sturt and Appila Tillites; overlies the Banda Siltstone.||26-APR-12
20188|Wilyerpa Formation|67870|5|Briefly described|p9|Neoproterozoic|Neoproterozoic|Adelaide Rift System.||Yudnamutana Subgroup.||||
20188|Wilyerpa Formation|67979|5|Briefly described|p536-7, p531 Fig.2, p542|Sturtian|Sturtian|In Central Flinders Ranges||Yudnamutana Subgroup||is overlain conformably by Tindelpina Shale Member (Tapley Hill Formation) in the Oraparinna area.|glacial|
20188|Wilyerpa Formation|68126|5|Briefly described|p31|Neoproterozoic|Neoproterozoic||||||Green siltstone.|
20188|Wilyerpa Formation|68270|5|Briefly described|p683,687|||Adelaide Rift Complex. U Pb zircon date of 659+\-6 Ma on an ash bed within the Wilyerpa Fm (Sturt glacial unit) (Fanning and Link 2008), consistent with age from black shales of the Aralka Formation and Re-Os dates from post-Sturt glacial shale units that paraconformably overlie diamictites in the Adelaide Rift Complex (643+\-2.4 Ma; Kendall et al. 2006) and NW Tasmania (640.7+\-4.7 Ma; Kendall et al. 2007).||||||
20188|Wilyerpa Formation|68276|6|Mentioned|p69|||Flinders Ranges.|||||Dominantly diamictite.|
20188|Wilyerpa Formation|69019|4|Described|p41, p45-46.|Neoproterozoic|Neoproterozoic|Of Dalgarno and Johnson (1966). A thick, largely marine clastic succession representing the waning stages of Sturtian glaciation in the Yudnamutana Trough. From <400 m to 584 m thick. Clast source areas from the E (Curnamona Province).||Unit in Yudnamutana Subgroup.||Conformably overlies Bolla Bollana Tillite; unconformably overlies Myrtle Springs Formation. Is equivalent to Lyndhurst Formation. Is overlain unconformably by Tapley Hill Formation.|Interbedded greenish siltstone, quartzite (meta-sandstone) and diamictite; glacial dropstones in lower third; minor interbeds of sandy and pebbly dolomite in upper third; all intervals have some turbidite character.|
20188|Wilyerpa Formation|69873|5|Briefly described|p82|||Adelaide Rift Complex. Included in diagram showing Cryogenian-Ediacaran stratigraphy and correlations with Tasmanian succession.|659 +/- 6 Ma (Fanning and Link, 2008).|||Correlative of Sturt Tillite.||
20188|Wilyerpa Formation|70031|5|Briefly described|p245-246|Cryogenian|Cryogenian|Adelaide Geosyncline. Associated with Sturtian glaciation; displays ice-rafted debris and marks the waning stage of Sturtian glaciation. Tuffaceous beds from lower Wilyerpa provide U-Pb zircon age of ca. 659 Ma (Fanning and Link 2008).||Unit of Yudnamutana Subgroup.|Includes Warcowie Dolomite Member.|Overlain by Tindelpina Shale Member/Tapley Hill Formation/Nepouie Subgroup. Underlain by Warcowie Dolomite Member and Benda Siltstone.||
20188|Wilyerpa Formation|70082|6|Mentioned|p2-3|Cryogenian|Cryogenian|Flinders Ranges. Contains marine till. U-Pb date of 659+\-6 Ma for a tuff low in the Wilyerpa Formation (Fanning and Link, 2008).||||||
20188|Wilyerpa Formation|70323|4|Described|p212-215,218-222|Cryogenian|Cryogenian|Central Flinders Ranges, Adelaide Geosyncline. Associated with Sturtian glaciation. Thickness: over 2.5km. Lithologically homogenous laterally and up-section, and contains lonestones, interpreted as ice-rafted dropstones and diagnostic of glaciogenic successions. The lower Wilyerpa section contains common dolomite beds, as well as lithified clasts (lonestones) of laminated hematite and jasper facies from the underlying Holowilena Ironstone.|c. 660 Ma|Unit of Yudnamutana Subgroup.|Includes Warcowie Dolomite Member.|Overlain by Tapley Hill Formation/Nepouie Subgroup. Underlain by Holowilena Ironstone.|Massive and stratified diamictites and shales/siltstones with common lonestones interbedded with sandstones, dolomite, dolomitic siltstones, and shales.|
20188|Wilyerpa Formation|70339|5|Briefly described|map legend|Neoproterozoic|Neoproterozoic||||||Siltstone, green. Lower third is fine grained, includes glacial dropstones; middle unit is medium to coarse sandstone; upper unit is siltstone with minor sandstone. Minor diamictite, sandy and pebbly dolomite.|
20188|Wilyerpa Formation|70405|6|Mentioned|p51 Table 4, p14 figure 6|Neoproterozoic|Neoproterozoic|||Yudnamutana Subgroup|||Siltstone, sandstone and diamictite.|
20188|Wilyerpa Formation|70407|5|Briefly described|p103 Fig 2|Neoproterozoic|Neoproterozoic|Age: Sturtian.||Of Umberatana Group.||Unconformably overlain by Tindelpina Shale.||
20188|Wilyerpa Formation|70657|5|Briefly described|p9 Fig.3, p54|Neoproterozoic|Neoproterozoic|||Yudnamutana Subgroup||Unconformably overlies Benda Siltstone.|Siltstone, sandstone, diamictite.|
20188|Wilyerpa Formation|70658|5|Briefly described|p14|Neoproterozoic|Neoproterozoic|||Yudnamutana Subgroup.|||Siltstone, sandstone, diamictite.|
20188|Wilyerpa Formation|70819|5|Briefly described|p11, 13, 29|Neoproterozoic|Neoproterozoic|Clare Valley. Deposited in the waning stages of the Sturtian Glaciation.|659 +/- 6 Ma (U-Pb).|Yudnamutana Subgroup.||Overlies Appila Tillite. Is overlain by Tapley Hill Formation.|Post-glacial bedded siltstones and sandstones.|
20188|Wilyerpa Formation|71129|5|Briefly described|p127|Cryogenian|Cryogenian|Of Stuart Shelf. Contains a 659+\-6 Ma tuff layer (U-Pb zircon; Fanning and Link 2008).||||Overlain by Whyalla Sandstone.||
20188|Wilyerpa Formation|71237|14|Not recorded|p10|||||||||
20188|Wilyerpa Formation|72449|5|Briefly described|p1, p2 Map Legend|Neoproterozoic|Neoproterozoic|||||Overlies Holowilena Ironstone and underlies Tapley Hill Formation.|Green siltstone, weathering buff yellow ln lower half, with intervals containing glacial dropstones. Middle section includes thick beds of storm deposited sandstone and glacial conglomerate.|
20188|Wilyerpa Formation|72456|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Marree 1:250k map sheet.|||||Siltstone, green. Lower third is fine-grained includes glacial dropstones; middle unit is medium to coarse sandstone: upper unit is siltstone with minor sandstone. Minor diamictite, sandy to pebbly dolomite.|
20188|Wilyerpa Formation|72473|6|Mentioned|p4-5|||Probably deposited during the second Sturtian glaciation. Exposed between the Oraparinna and Enorama Diapirs in the central Flinders zone.||||Underlain by Holowilena Ironstone.|Dominantly mudstone, shale, siltstone, and arenites with minor tillite and pebbly mudstone.|
20188|Wilyerpa Formation|72601|6|Mentioned|p6||Cryogenian|Adelaide Rift Complex. Geochronologic constraint: see Fanning and Link (2008), Preiss et al. (2011).|659 +/- 6 Ma|||||
20188|Wilyerpa Formation|73093|5|Briefly described|map legend|Neoproterozoic|Neoproterozoic||||||Interbedded siltstone and sandstone. Minor diamictite, sandy and pebbly dolomite.|12-DEC-21
20188|Wilyerpa Formation|73227|6|Mentioned|p24|Cryogenian|Cryogenian|Adelaide Rift Complex.|663.03 +/- 0.11 Ma U-Pb|||Overlain by Tapley Hill Formation.||
20188|Wilyerpa Formation|73234|5|Briefly described|p20-21|Cryogenian|Cryogenian|Age is of a volcaniclastic layer reported by Cox et al. (2018). Previous age from a tuffaceous horizon of 659 +/- 6 Ma was reported by Fanning and Link (2008). Pyroclastic zircons most probably [sourced from] eastern Antarctica.|663.03 +/- 0.11 Ma CA-ID-TIMS U-Pb|Umberatana Group||Underlain by Bolla Bollana Tillite.|Glaciogenic.|
20188|Wilyerpa Formation|74367|5|Briefly described|p7 Fig.6, p18-19, p20-21|Cryogenian|Cryogenian||663.03+/-0.11 Ma zircon U-Pb CA-ID-TIMS|Yudnamurtana Subgroup||||
20219|Windermere Sandstone Member|12781|6|Mentioned|p386|Early Cretaceous|Early Cretaceous|Otway Basin. Maximum thickness 21m.||Eumeralla Formation.||Unconformably overlies Katnook Sandstone.||
20219|Windermere Sandstone Member|22674|5|Briefly described|Fig.2 p719|Aptian|Aptian|Part of Otway Supergroup.||||||16-OCT-07
20219|Windermere Sandstone Member|22686|5|Briefly described|Fig3p745|||Basal sand unit of Eumeralla Formation. Shown only as Windermere Sandstone in Fig. 3.  Geological Province: Otway Basin.||||||17-JAN-06
20219|Windermere Sandstone Member|24314|5|Briefly described|p61 Fig.2|Aptian||Geological Province: Otway Basin. Max. Thickness 21m. Of the Otway Supergroup.||||||30-NOV-04
20219|Windermere Sandstone Member|24453|5|Briefly described|p809 Fig.2|Aptian|Aptian|Of Otway Group. Overlain by Eumeralla Formation. Geological Province: Otway Basin.||||||07-FEB-11
20219|Windermere Sandstone Member|24551|5|Briefly described|p251|||||||||
20219|Windermere Sandstone Member|42361|3|Fully described|p9|Aptian||||||||
20219|Windermere Sandstone Member|42545|5|Briefly described|Fig.4 P15|||||||||
20219|Windermere Sandstone Member|43171|6|Mentioned|5-8|||Of Eumeralla Formation. Age: 120-125Ma||||||
20219|Windermere Sandstone Member|43195|5|Briefly described|Map Legend||Early Cretaceous|See also commentary on back of map.Of Crayfish Group.||||||
20219|Windermere Sandstone Member|43733|6|Mentioned|Fig.2.11,p65||Early Cretaceous|||||||
20219|Windermere Sandstone Member|43744|6|Mentioned|Fig.3,p3|||||||||
20219|Windermere Sandstone Member|43814|6|Mentioned|Fig.3,p115|||||||||
20219|Windermere Sandstone Member|44133|5|Briefly described|p144|Aptian|Aptian|Geological Province: Otway Basin. Of the Eumeralla Formation. Thickness: 100m.||||||
20219|Windermere Sandstone Member|61017|6|Mentioned|p6|||||||||07-FEB-11
20219|Windermere Sandstone Member|61329|6|Mentioned|p121|||||||||
20219|Windermere Sandstone Member|61547|6|Mentioned|p461 Fig.2. |Barremian|Barremian|||Unit in Eumeralla Formation.||Overlies unconformably the Katnook Sandstone.||
20219|Windermere Sandstone Member|61622|5|Briefly described|p436 Fig. 2|Cretaceous|Cretaceous|Otway Supergroup. Geological Province: Otway Basin.||||||07-FEB-11
20219|Windermere Sandstone Member|61627|5|Briefly described|p500 Fig. 2|Early Cretaceous|Early Cretaceous|Of Eumeralla Formation. Geological Province: Otway Basin.||||||07-FEB-11
20219|Windermere Sandstone Member|63122|5|Briefly described|p17 Fig. 4.3|Aptian|Barremian|Of Eumeralla Formation (Otway Supergroup). Geological Province: Otway Basin.||||||
20219|Windermere Sandstone Member|63124|3|Fully described|p48 Fig. 5.1, p49 Fig. 5.2, p73|Barremian|Barremian|Supersedes Windemere Member. Of Eumeralla Formation. Unconformable over Crayfish Group. Age: 125-119Ma. Max. thickness: 16m; 160m in Victoria. Geological Province: Otway Basin.Crayfish Group.||||||31-JAN-08
20219|Windermere Sandstone Member|63125|6|Mentioned|p116 Tb.7.6, p121 Tb. 7.11|||Geological Province: Otway Basin||||||
20219|Windermere Sandstone Member|63129|5|Briefly described|p127, p132|||Of the Otway Supergroup. Max. thickness: 16m. Geological Province: Otway Basin.||||||30-JAN-08
20219|Windermere Sandstone Member|63267|5|Briefly described|p485 Fig.2, p496|Early Cretaceous|Early Cretaceous|Penola Trough, Otway Basin. Abbreviated to Windermere Sandstone on p496.||Eumeralla Formation.||Unconformably overlies Katnook Sandstone.||
20219|Windermere Sandstone Member|63431|5|Briefly described|p677 Fig. 2|Barremian|Barremian|Of the Eumeralla Formation (Otway Supergroup). Geological Province: Penola Trough/Otway Basin.||||||07-FEB-11
20219|Windermere Sandstone Member|69948|6|Mentioned|Fig.4.2|||Otway Basin (a rift basin). Sediment thickness, sonic log, gamma ray log all shown in contrast with Eromanga Basin (an intracratonic basin).||Eumeralla Formation.||Overlies Katnook Sandstone.||
20219|Windermere Sandstone Member|70077|5|Briefly described|Regional: Fig.4|Aptian|Aptian|Otway Basin: Robe-Penola Trough.||Eumeralla Formation.||Overlies Katnook Sandstone.||
20219|Windermere Sandstone Member|71342|6|Mentioned|Ch4 p9 Fig 4.2|||Otway Basin.||||||
20219|Windermere Sandstone Member|72050|5|Briefly described|p235-236|Aptian|Aptian|Kopsen and Scholefield (1990).||Basal Eumeralla Formation.||Unconformably overlies Katnook Sandstone.|Quartzose sandstone.|
20250|Winnambool Formation|2967|5|Briefly described|p14, p15 Fig.2.2, p24, 42|Miocene|Miocene|Western Murray Basin.||Murray Group.||Overlies Geera Clay and Duddo Limestone (and grades into the latter). Is separated from the overlying Bookpurnong beds by the Mologa Surface.||
20250|Winnambool Formation|10010|5|Briefly described|p12 Fig. 3|Middle Miocene|Late Oligocene|Of the Murray Group. Geological Province: Murray Basin.||||||13-AUG-07
20250|Winnambool Formation|22587|6|Mentioned|p79 Fig.7|Middle Miocene|Late Oligocene|||||||
20250|Winnambool Formation|22773|5|Briefly described|p351,Fig24.8p352|Miocene||||||||
20250|Winnambool Formation|22799|2|Defined|p33|Early Miocene|Late Oligocene|||||||
20250|Winnambool Formation|22857|5|Briefly described|p351, p352 Fig. 24.8|Miocene|Oligocene|Of the Murray Group. Geological Province: Murray Basin. See also p353 Fig. 24.9.||||||
20250|Winnambool Formation|22887|5|Briefly described|Fig.6 p13|Middle Miocene||||||||
20250|Winnambool Formation|22893|5|Briefly described|fig4 p9|Miocene|Miocene|||||||
20250|Winnambool Formation|23179|6|Mentioned|Fig.2|Middle Miocene|Late Oligocene|Murray Supergroup||||||
20250|Winnambool Formation|23226|6|Mentioned|p889,890,891,897|||Of Murray Supergroup.||||||
20250|Winnambool Formation|23884|5|Briefly described|p153, p155 Fig. 13.2|Middle Miocene|Middle Miocene|Geological Province: Murray Basin.||||||21-SEP-09
20250|Winnambool Formation|23909|6|Mentioned|p298|||||||||
20250|Winnambool Formation|23921|5|Briefly described|p1109|Middle Miocene|Middle Miocene|Geological Province: Murray Basin.||||||
20250|Winnambool Formation|24551|6|Mentioned|p322 Fig 10.29, p731 Table 17.1|||Of the Murray Group. Max. Thickness: 130m.||||||
20250|Winnambool Formation|24563|5|Briefly described|p485|||Included in the Murray Supergroup by Lukasik and James (1998).  However, Murray Supergroup now abandoned and Murray Group reinstated - Winnambool Formation not included.  Geological Province: Murray Basin.||||||
20250|Winnambool Formation|29591|6|Mentioned|Table 20|||||||||
20250|Winnambool Formation|29898|6|Mentioned|p216|||||||||
20250|Winnambool Formation|30581|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
20250|Winnambool Formation|30934|6|Mentioned|Map legend|Miocene|Miocene|||||||
20250|Winnambool Formation|30935|6|Mentioned|Map legend|Tertiary|Tertiary|Subsurface||||||
20250|Winnambool Formation|30936|6|Mentioned|Map legend|Oligocene|Oligocene|||||||
20250|Winnambool Formation|31741|6|Mentioned|p6|||||||||
20250|Winnambool Formation|31743|6|Mentioned|p8|||||||||
20250|Winnambool Formation|31746|4|Described|p196|||||||||
20250|Winnambool Formation|31747|6|Mentioned|Map legend|Miocene|Oligocene|Oligocene - Miocene||||||
20250|Winnambool Formation|34735|4|Described|p33|||Also mentioned on P32.||||||
20250|Winnambool Formation|34813|6|Mentioned|p62|||||||||
20250|Winnambool Formation|35285|5|Briefly described|p413|||||||||
20250|Winnambool Formation|37809|6|Mentioned|p7|||See also P7.||||||
20250|Winnambool Formation|39329|6|Mentioned|Fig.1|||||||||
20250|Winnambool Formation|39929|6|Mentioned|p268|||||||||
20250|Winnambool Formation|40820|6|Mentioned|Fig.4|||||||||
20250|Winnambool Formation|41511|6|Mentioned|p20|||||||||
20250|Winnambool Formation|41868|5|Briefly described|p551|||||||||
20250|Winnambool Formation|42125|5|Briefly described|p136|||See also Fig.5||||||
20250|Winnambool Formation|42126|6|Mentioned|p151|||||||||
20250|Winnambool Formation|42130|6|Mentioned|Fig.3 P265|||||||||
20250|Winnambool Formation|42133|6|Mentioned|p301|||||||||
20250|Winnambool Formation|42134|6|Mentioned|Fig.3 P335|||||||||
20250|Winnambool Formation|42137|4|Described|p371|||See also Table 2||||||
20250|Winnambool Formation|42138|6|Mentioned|p388|||||||||
20250|Winnambool Formation|42827|4|Described|p270|||||||||
20250|Winnambool Formation|42881|4|Described|Fig.3, P84|||||||||
20250|Winnambool Formation|42966|2|Defined|p146|Middle Miocene|Late Oligocene|Of the  Murray Group.||||||29-JUL-08
20250|Winnambool Formation|43655|5|Briefly described|p40-846|||||||||
20250|Winnambool Formation|43780|6|Mentioned|p5|Middle Miocene|Late Oligocene|||||||
20250|Winnambool Formation|43790|5|Briefly described|p383|||||||||
20250|Winnambool Formation|43791|5|Briefly described|p371|||||||||
20250|Winnambool Formation|43804|6|Mentioned|Fig.2,p49|||||||||
20250|Winnambool Formation|44133|5|Briefly described|p159|Middle Miocene|Early Miocene|Of the Murray Group. Geological Province: Murray Basin.||||||
20250|Winnambool Formation|44191|5|Briefly described|Map Legend|Middle Miocene|Early Oligocene|||||||
20250|Winnambool Formation|49038|4|Described|Table 2|||||||||
20250|Winnambool Formation|49040|6|Mentioned|p11|||||||||
20250|Winnambool Formation|50154|5|Briefly described|p135|||Of the Murray Group.||||||
20250|Winnambool Formation|60538|5|Briefly described|p480 Fig. 19|||Geological Province: Murray Basin.||||||
20250|Winnambool Formation|61155|5|Briefly described|p4, p18|Middle Miocene||Of the Murray Group. Platform/lagoonal deposits - calcareous clays. Interfingers with and grades into Geera Clay; interfingers with Duddo Limestone. Geological Province: Murray Basin.||||||
20250|Winnambool Formation|61314|5|Briefly described|p129|||Shallow water equivalent of Duddo Limestone in the eastern part of the basin. Geological Province: Murray Basin.||||||
20250|Winnambool Formation|63066|5|Briefly described|p485|||Revised stratigraphy of Lukasik and James (1999) incorporates this unit, the Ettrick Formation and Geera Clay into their new Murray Supergroup.  These were not formerly included in the definition of the Murray Group.||||||08-FEB-07
20250|Winnambool Formation|63460|5|Briefly described|p838, p839 Fig. 2b|||Of Lawrence and Abele (1976). Geological Province: Murray Basin.||||||06-FEB-09
20250|Winnambool Formation|63777|6|Mentioned|p1104 Fig. 1, p1105|||Geological Province: Murray Basin.||||||18-MAR-09
20250|Winnambool Formation|63887|5|Briefly described|p20, p21 Fig. 1|Middle Miocene|Late Oligocene|Of Murray Group. Marl.||||||
20250|Winnambool Formation|64237|5|Briefly described|p17, p19|Middle Miocene|Early Miocene|Of Lawrence (1966). Retained as a formal unit through the Lawrence (1975) and Lawrence and Abele(1988) revisions where it overlay the Geera Clay.  Became constituent in Murray Supergroup (Lukasic and James 1998), then retained in reinstateed Murray Group.||||||03-FEB-09
20250|Winnambool Formation|64823|5|Briefly described|p1011|Cenozoic|Cenozoic|Overlies Renmark Group. Terrestrial sands and gravels  Geological province: Murray Basin.||||||
20250|Winnambool Formation|65552|5|Briefly described|p5 Fig. 3, p6|Middle Miocene|Early Oligocene|Also spelt Winambool Formation in text. Murray Basin unit. Deposited contemporaneously with other Murray Basin units including Murray Group to the west and Geera Clay and Olney Formation to the east. Unconformably underlies Bookpurnong beds.||||||
20250|Winnambool Formation|67462|5|Briefly described|Map legend.|Miocene|Miocene|Murray Basin.||Unit in Murray Group.||||
20250|Winnambool Formation|68140|6|Mentioned|p1700-1701|Neogene|Paleogene|Middle Tertiary age.||||||09-FEB-18
20250|Winnambool Formation|68189|5|Briefly described|p27 Tb.3.2, p29|Miocene|Miocene|Maximum flooding surface.||Of the Murray Group.||Underlain by the Olney Formation. Overlain by the Parilla Sand.||
20250|Winnambool Formation|68715|5|Briefly described|p31 Fig.5|Burdigalian|Burdigalian|Murray Basin.||Of the Murray Group.||||
20250|Winnambool Formation|68716|6|Mentioned|p39 Fig.3|||||||Overlain by the Pata Formation. Underlain by the Glenforslan Formation.||
20250|Winnambool Formation|70718|5|Briefly described|p24-p25, p103|Middle Miocene|Late Oligocene|Murray Basin. Deposited in a lagoonal environment.||Of Murray Group.|||Marly limestone with thin interbeds of grey skeletal calcsiltite and calcarenite.|30-MAY-19
20250|Winnambool Formation|70961|14|Not recorded|p136|||Geological section.||||||
20250|Winnambool Formation|71593|5|Briefly described|p52, p54|Miocene|Oligocene|Murray Basin.||Murray Group||Interfingered with the Geera Clay, Olney Formation and the Calivil Formation.|Muddy shallow marine marl.|
20250|Winnambool Formation|72445|5|Briefly described|App.1, App.2; App.6 p2; App.7 p7 Fig.4.|Miocene|Late Oligocene|Shown in App 7 Fig 4 (from Brown & Stephenson 1991). App.2 is a .csv format file. Identified in Stavely 12,16.||Murray Group||Overlain gradationally by Geera Clay. Overlies Renmark Group (sharp contact). Shown as unconformably underlying Bookpurnong beds.|Includes glauconitic marl and mud; glauconitic marl with limestone nodules or beds. marl, mud and limestone.|
20250|Winnambool Formation|73118|5|Briefly described|p53, 64, 82|Miocene|Oligocene|Glenelg Zone, Western Victoria. Drill core summary log. Abundant well-preserved and diverse faunas. Restricted-marine and lagoonal environments. 110m thick; mainly <50m.||Murray Group.||Overlies Olney Formation. Is overlain by Loxton-Parilla Sands.|Poorly consolidated, grey to green, glauconitic, highly fossiliferous calcareous clay (marl); intercalated skeletal calc-siltite, calcarenite, and dense micritic limestone.|
20250|Winnambool Formation|73228|4|Described|p50-51, p55-57, p60|Middle Miocene|Late Early Oligocene|Murray Basin. Shallow-water restricted marine and lagoonal facies. Mostly deposited adjacent to an estuarine environment due to the abundance of marine dinoflagellate cysts and freshwater algae.||Murray Group|||Grey to light green fossiliferous marl, glauconitic marly limestone and marly clay.|
20250|Winnambool Formation|73229|5|Briefly described|p66-67, p70|Middle Miocene|Mid Oligocene|Murray Basin. [Analysed using pXRF; see article]. Shallow water, restricted marine and lagoonal.||Murray Group|||Includes marl, fossiliferous; glauconitic marly limestone; marly clay.|
20268|Winton Formation|12597|5|Briefly described|p492 Tb.1, p500, p501|Cenomanian|Cenomanian|Eromanga Basin. 400-700m, locally up to 1200m, thick.||||Overlies Mackunda Formation.|Basal paralic-nonmarine transition zone, overlain by non-marine sequence of fine- to medium-grained labile sandstone, siltstone, mudstone and lenticular coal seams.|
20268|Winton Formation|13497|5|Briefly described|p13, p115, p115 fig 6.33|Late Cretaceous|Late Cretaceous|Eromanga Basin. Deposited in a high-sinuosity fluvial environment. See also p144, p144 fig 9.2, p146, p148-p154, .||||Overlies the Mackunda Formation and the Oodnadatta Formation. Unconformably overlain by the Mount Howie Sandstone and the Eyre Formation.|Sandstone, siltstone, shale and coal.|
20268|Winton Formation|13516|6|Mentioned|p167 fig 10, p169 fig 11, p171 fig 12|Late Cretaceous|Late Cretaceous|In Eromanga Basin.||||||
20268|Winton Formation|22464|6|Mentioned|p9||Late Cretaceous|Also p8. In the Eromanga Basin.||||||19-DEC-06
20268|Winton Formation|22587|5|Briefly described|p71|Cenomanian|Albian|In the Eromanga Basin.||||||19-DEC-06
20268|Winton Formation|22773|6|Mentioned|p338|||||||||
20268|Winton Formation|22839|6|Mentioned|P33|||||||||
20268|Winton Formation|22857|4|Described|p296-7 Tb 22.1, p326, p552 Tb A1.13|Cenomainian|Cenomainian|Of the Rolling Downs Group. Interbedded mudstone and lithic and feldspathic arenite. Max. thickness: 400m in NSW. Geological Province: Eromanga Basin. See also p312-3 Fig. 22.6.||||||
20268|Winton Formation|22862|6|Mentioned|p327||Cenomanian|||||||
20268|Winton Formation|22865|4|Described|p314,Table22.1p296-7|Cenomanian|Cenomanian|||||||
20268|Winton Formation|22883|5|Briefly described|P31, Fig2||Late Cretaceous|Underlying unit is Mackunda Formation.||||||19-DEC-06
20268|Winton Formation|22912|6|Mentioned|34|||Geological province: Eromanga Basin.||||||19-DEC-06
20268|Winton Formation|23054|6|Mentioned|Fig5p22|||||||||
20268|Winton Formation|23056|6|Mentioned|9|||Geol province Eromanga Basin. Parent Rolling Downs Group||||||
20268|Winton Formation|23154|5|Briefly described|Map Legend|Late Cretaceous|Late Cretaceous|Geological Province - Eromanga Basin. Of the Neales River Group.||||||19-DEC-06
20268|Winton Formation|23155|4|Described|p33|Late Cretaceous|Early Cretaceous|Uppermost Eromanga Basin unit known on STRZELECKI, and is disconformably overlain by Tertiary Eyre Formation.||||||19-DEC-06
20268|Winton Formation|23375|5|Briefly described|Fig2 p265||Cenomanian|In the Eromanga Basin.||||||19-DEC-06
20268|Winton Formation|23425|5|Briefly described|Plate 10.2|||Eromanga Basin Province.||||||
20268|Winton Formation|23818|5|Briefly described|p141 Fig.65, p144 Fig.66|Cenomanian|Cenomanian|Geological Province: Cooper Basin. Of the Manuka Sub-Group. Max. thickness: >2000 ft.||||||18-APR-05
20268|Winton Formation|23830|5|Briefly described|Fig. 3a|Cretaceous|Cretaceous|Geological Province: Boorthanna Trough, eastern Arckaringa Basin.||||||24-JAN-06
20268|Winton Formation|23883|5|Briefly described|p129 Fig. 11.2|Cretaceous|Cretaceous|Of Rolling Downs Group.  Geological Province: Great Australian Superbasin.||||||
20268|Winton Formation|23911|5|Briefly described|p97 Fig. 11|Cretaceous|Cretaceous|Geological Province: Eromanga Basin. Of the Rolling Downs Group.||||||
20268|Winton Formation|23916|5|Briefly described|p523|Cenomanian|Albian|Geological Province: Eromanga Basin.||||||
20268|Winton Formation|23982|5|Briefly described|p35 Fig.7|Cretaceous|Cretaceous|Of Rolling Downs Group. Geological Province: Great Artesian Basin.||||||
20268|Winton Formation|24092|5|Briefly described|p5|Cretaceous|Cretaceous|Geological Province: Great Artesian Basin.||||||
20268|Winton Formation|24112|5|Briefly described|p270|Cenomanian|Albian|Age: 97-90Ma (Krieg et al, 1995). Geological Province: Eromanga Basin||||||
20268|Winton Formation|24175|3|Fully described|p30, p17 Fig. 3|Cenomanian|Albian|Overlain by Eyre Formation; conformably overlies Mackunda Formation.  Max. thickness: 88m.  Geological Province: Eromanga Basin.||||||
20268|Winton Formation|24204|5|Briefly described|p263 Fig.4, p267|Late Cretaceous|Late Cretaceous|Geological Province: Eromanga Basin.||||||17-DEC-04
20268|Winton Formation|24210|5|Briefly described|p133 Fig. 2|Late Cretaceous|Late Cretaceous|Geological Province: Eromanga Basin.||||||
20268|Winton Formation|24243|5|Briefly described|p3 Fig.2|Cretaceous|Cretaceous|Of Rolling Downs Group.||||||
20268|Winton Formation|24251|5|Briefly described|p234 Fig.1|Cenomanian|Cenomanian|Geological Province: Eromanga Basin||||||
20268|Winton Formation|24321|5|Briefly described|Map legend|Cenomanian|Cenomanian|Of the Neales River Group.||||||19-DEC-06
20268|Winton Formation|29591|6|Mentioned|p71|||||||||
20268|Winton Formation|29721|6|Mentioned|Table 137|||||||||
20268|Winton Formation|30019|6|Mentioned|p2|||||||||
20268|Winton Formation|30055|6|Mentioned|p159|||||||||
20268|Winton Formation|30102|6|Mentioned|Table 4|||See also p36,37.||||||19-DEC-06
20268|Winton Formation|30104|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower to Upper? Cretaceous||||||
20268|Winton Formation|30514|6|Mentioned|p102|||Middle Cretaceous age.||||||
20268|Winton Formation|30539|6|Mentioned|p7|||Late Albian - early Cenomanian age||||||
20268|Winton Formation|30540|6|Mentioned|Fig.6|||||||||
20268|Winton Formation|30691|4|Described|p17|||See also p21,Table 4. Lower - Upper Cretaceous||||||19-DEC-06
20268|Winton Formation|30700|6|Mentioned|p28|||||||||
20268|Winton Formation|30803|6|Mentioned|p2|||Cretaceous age||||||
20268|Winton Formation|30804|6|Mentioned|p7|||On Table 1. See also Table 2.||||||
20268|Winton Formation|30807|6|Mentioned|p102|||Suggested map symbol||||||
20268|Winton Formation|30853|5|Briefly described|Table 3|||Lower to Upper Cretaceous||||||
20268|Winton Formation|30854|4|Described|Table 4|||Lower to Upper Cretaceous age.||||||19-DEC-06
20268|Winton Formation|30855|6|Mentioned|Map legend|Cretaceous|Cretaceous|Unit in Rolling Downs Group.||||||19-DEC-06
20268|Winton Formation|30856|4|Described|Table 3|||On p10. Lower-Upper Cretaceous.||||||19-DEC-06
20268|Winton Formation|30857|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower - Upper Cretaceous||||||
20268|Winton Formation|30914|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
20268|Winton Formation|30918|6|Mentioned|p82|||||||||
20268|Winton Formation|30919|6|Mentioned|Map legend|Cenomanian|Albian|Albian - Cenomanian||||||
20268|Winton Formation|30921|6|Mentioned|Map legend|Oligocene|Oligocene|||||||
20268|Winton Formation|31144|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|L. - U. Cretaceous||||||
20268|Winton Formation|31145|5|Briefly described|Table 1|||L. - U. Cretaceous||||||
20268|Winton Formation|31425|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower-Upper? Cretaceous||||||
20268|Winton Formation|31430|5|Briefly described|Table 1|||L.-U.Cretaceous||||||
20268|Winton Formation|31431|5|Briefly described|Table 3|||L.Cretaceous||||||
20268|Winton Formation|31432|4|Described|Table 1|||L.-U.Cretaceous||||||
20268|Winton Formation|31436|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower to Upper Cretaceous||||||
20268|Winton Formation|31438|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower to Upper Cretaceous||||||
20268|Winton Formation|31441|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower - Upper Cretaceous||||||
20268|Winton Formation|31443|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
20268|Winton Formation|31553|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower - Upper Cretaceous||||||
20268|Winton Formation|31649|6|Mentioned|p63|||||||||
20268|Winton Formation|31699|4|Described|p133|||Middle Cretaceous||||||
20268|Winton Formation|31706|6|Mentioned|p669|||Cretaceous correlation chart||||||
20268|Winton Formation|31923|6|Mentioned|p15|||||||||
20268|Winton Formation|32274|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
20268|Winton Formation|32275|6|Mentioned|p6|||||||||
20268|Winton Formation|32277|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower Cretaceous - Upper Cretaceous.||||||
20268|Winton Formation|32314|6|Mentioned|Fig. 4|||||||||
20268|Winton Formation|32396|6|Mentioned|p10|||Equivalents||||||
20268|Winton Formation|32413|6|Mentioned|p103|||||||||
20268|Winton Formation|32472|6|Mentioned|p17|||||||||
20268|Winton Formation|32618|6|Mentioned|Table 1|||Perm. Strat. table.||||||
20268|Winton Formation|32696|6|Mentioned|Fig.4|||||||||
20268|Winton Formation|32796|6|Mentioned|p303|||||||||
20268|Winton Formation|32918|6|Mentioned|p20|||||||||
20268|Winton Formation|33016|6|Mentioned|p1|||Table on P1||||||
20268|Winton Formation|33017|6|Mentioned|Table 1|||||||||
20268|Winton Formation|33067|4|Described|Table 1|Late Cretaceous|Early Cretaceous|Of the Rolling Downs Group.||||||07-JUL-04
20268|Winton Formation|33069|4|Described|p7|||||||||
20268|Winton Formation|33072|4|Described|Table 1|||L.Cret.||||||
20268|Winton Formation|33073|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
20268|Winton Formation|33075|6|Mentioned|Table 1|||||||||
20268|Winton Formation|33078|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower - Upper? Cretaceous||||||
20268|Winton Formation|33079|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower - Upper Cretaceous||||||
20268|Winton Formation|33081|6|Mentioned|p26|||||||||
20268|Winton Formation|33082|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower - Upper Cretaceous||||||
20268|Winton Formation|33083|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower - Upper Cretaceous||||||
20268|Winton Formation|33086|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower to Upper Cretaceous||||||
20268|Winton Formation|33087|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower - Upper Cretaceous||||||
20268|Winton Formation|33088|4|Described|Table 3|||Of the Rolling Downs Group.||||||19-DEC-06
20268|Winton Formation|33089|4|Described|Table 2|||L.-U.Cret.||||||
20268|Winton Formation|33095|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower - Upper Cretaceous||||||
20268|Winton Formation|33165|6|Mentioned|Chart|||Correlation chart only||||||
20268|Winton Formation|33368|6|Mentioned|p25|||Strat.Table.||||||
20268|Winton Formation|33372|6|Mentioned|Table 1|||||||||
20268|Winton Formation|33414|6|Mentioned|p212-214,Tb.||Cenomanian|Part of Manuka Sub-Group.||||||
20268|Winton Formation|33448|4|Described|Table 1|||L.-U.Cret.||||||11-JAN-10
20268|Winton Formation|33449|4|Described|Table 1|||L.-U.Cret.||||||
20268|Winton Formation|33452|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower to Upper Cretaceous||||||
20268|Winton Formation|33490|6|Mentioned|p30|||Cret. sediments. Correlation||||||
20268|Winton Formation|33521|6|Mentioned|p10|||Upper Cretaceous||||||
20268|Winton Formation|33561|6|Mentioned|p102|||||||||
20268|Winton Formation|33569|6|Mentioned|p63|||||||||
20268|Winton Formation|33639|5|Briefly described|p12|||L.-U.Cret.||||||
20268|Winton Formation|33640|4|Described|Table 2|||L.-U.Cret.||||||
20268|Winton Formation|33642|6|Mentioned|p144-45,147,148,Tb.1|||Refers Dunstan (1916) & Whitehouse (1954)||||||
20268|Winton Formation|33647|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower - Upper? Creataceous||||||
20268|Winton Formation|33648|6|Mentioned|p19|||Stratigraphy.||||||
20268|Winton Formation|33819|6|Mentioned|p1|||||||||
20268|Winton Formation|33820|6|Mentioned|Map legend|Cenomanian|Albian|Albian - Cenomanian||||||
20268|Winton Formation|33821|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
20268|Winton Formation|33822|6|Mentioned|Map legend|Cenomanian|Albian|Albian - Cenomanian||||||
20268|Winton Formation|33823|6|Mentioned|Map legend|Cenomanian|Neocomian|Neocomian - Cenomanian||||||
20268|Winton Formation|33824|6|Mentioned|p7|||P12, Tables 1 & 2||||||
20268|Winton Formation|33825|6|Mentioned|p8|||Strat. table. Lithology||||||
20268|Winton Formation|33827|6|Mentioned|p7|||See also p3 and Tables 1 and 3.||||||19-DEC-06
20268|Winton Formation|33828|6|Mentioned|p9|||See also Table 1||||||
20268|Winton Formation|33831|6|Mentioned|Map legend|Cenomanian|Neocomian|Neocomian - Cenomanian||||||
20268|Winton Formation|33832|6|Mentioned|p6|||Strat.||||||
20268|Winton Formation|33936|6|Mentioned|Fig.3A|||Cret.||||||
20268|Winton Formation|33937|6|Mentioned|p3|||||||||
20268|Winton Formation|33938|6|Mentioned|p19|||Refers Jack (1930).||||||
20268|Winton Formation|33964|4|Described|p6|||||||||
20268|Winton Formation|33971|5|Briefly described|p37|||See also Fig.15.||||||
20268|Winton Formation|34035|6|Mentioned|p544|||Cret.||||||
20268|Winton Formation|34061|6|Mentioned|p53|||||||||
20268|Winton Formation|34065|4|Described|p6|||L.-U. Cret.||||||
20268|Winton Formation|34174|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower - Upper Cretaceous||||||
20268|Winton Formation|34217|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|||||||
20268|Winton Formation|34218|4|Described|Table 1|||Lower - Upper Cretaceous. See also pp8,10-12 etc.||||||19-DEC-06
20268|Winton Formation|34254|6|Mentioned|p492|||||||||
20268|Winton Formation|34259|6|Mentioned|p451|||||||||
20268|Winton Formation|34282|6|Mentioned|p88|||See also PP90, 93 etc.||||||
20268|Winton Formation|34287|6|Mentioned|p199|||Cret.||||||
20268|Winton Formation|34356|6|Mentioned|p32|||||||||
20268|Winton Formation|34400|6|Mentioned|p14|||Lower Cretaceous||||||
20268|Winton Formation|34454|5|Briefly described|Table 1|||Cretaceous. See also pp6,12,15.||||||19-DEC-06
20268|Winton Formation|34485|5|Briefly described|Table 1|||Lower - Upper? Cretaceous.||||||19-DEC-06
20268|Winton Formation|34486|5|Briefly described|Table 1|||Lower - Upper? Cretaceous. See also Table 2||||||
20268|Winton Formation|34487|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower - Upper Cretaceous||||||
20268|Winton Formation|34543|6|Mentioned|p98|||||||||
20268|Winton Formation|34611|4|Described|p158|||Cretaceous. See Fig.65,66||||||
20268|Winton Formation|34909|6|Mentioned|p992|||||||||
20268|Winton Formation|34948|6|Mentioned|Fig. 70|||||||||
20268|Winton Formation|35067|6|Mentioned|Fig.4|||||||||
20268|Winton Formation|35139|6|Mentioned|p17|||||||||
20268|Winton Formation|35151|6|Mentioned|p147|||||||||
20268|Winton Formation|35239|6|Mentioned|p258|||||||||
20268|Winton Formation|35560|6|Mentioned|Fig.3|||||||||
20268|Winton Formation|35793|4|Described|p241|||Details of weathering and profiles.||||||
20268|Winton Formation|35811|5|Briefly described|Table 3|||||||||
20268|Winton Formation|35894|6|Mentioned|p275|||||||||
20268|Winton Formation|36172|6|Mentioned|Appendix|||||||||
20268|Winton Formation|36213|6|Mentioned|Fig.2|||||||||
20268|Winton Formation|36229|6|Mentioned|Map legend|Eocene|Eocene|||||||
20268|Winton Formation|36243|6|Mentioned|Table 6A|||||||||
20268|Winton Formation|36327|6|Mentioned|p7|||||||||
20268|Winton Formation|36571|6|Mentioned|p98|||See also Table 4.||||||
20268|Winton Formation|36912|6|Mentioned|Fig.3|||||||||
20268|Winton Formation|36922|6|Mentioned|Fig.3|||||||||
20268|Winton Formation|37065|5|Briefly described|p41|||||||||
20268|Winton Formation|37114|6|Mentioned|p308|||||||||
20268|Winton Formation|37116|4|Described|p312|||||||||
20268|Winton Formation|37261|6|Mentioned|p351|||||||||
20268|Winton Formation|37263|6|Mentioned|p319|||||||||
20268|Winton Formation|37287|6|Mentioned|p36|||||||||
20268|Winton Formation|37451|6|Mentioned|Table 2|||||||||
20268|Winton Formation|37603|6|Mentioned|p444|||||||||
20268|Winton Formation|37607|6|Mentioned|p333|||||||||
20268|Winton Formation|37608|3|Fully described|Table 1|||||||||
20268|Winton Formation|37776|6|Mentioned|Fig.2|||||||||
20268|Winton Formation|38068|5|Briefly described|p72|||||||||
20268|Winton Formation|38226|6|Mentioned|p414|||See also Fig.6.||||||
20268|Winton Formation|38373|6|Mentioned|p622|||||||||
20268|Winton Formation|38779|6|Mentioned|p3|||||||||
20268|Winton Formation|38814|6|Mentioned|Table 1|||||||||
20268|Winton Formation|39070|4|Described|p366|||||||||
20268|Winton Formation|39085|6|Mentioned|Fig.2|||||||||
20268|Winton Formation|39211|5|Briefly described|Fig.3, Fig.6|||See also Figs 4,5,7,14,15 etc. Correlation||||||
20268|Winton Formation|39352|6|Mentioned|Map legend|Albian|Aptian|Aptian to Albian||||||
20268|Winton Formation|39445|5|Briefly described|Table 11|||||||||
20268|Winton Formation|39478|6|Mentioned|Table 1|||||||||
20268|Winton Formation|39482|6|Mentioned|Fig.7|||||||||
20268|Winton Formation|39846|6|Mentioned|Fig.2|||||||||
20268|Winton Formation|39847|5|Briefly described|p40|||||||||
20268|Winton Formation|39914|6|Mentioned|p3|||||||||
20268|Winton Formation|39943|6|Mentioned|Table 8A|||||||||
20268|Winton Formation|40003|6|Mentioned|Fig.9   or|||||||||
20268|Winton Formation|40058|6|Mentioned|Fig.1|||||||||
20268|Winton Formation|40121|6|Mentioned|Table 1|||||||||
20268|Winton Formation|40150|6|Mentioned|p77|||||||||
20268|Winton Formation|40199|6|Mentioned|p16|||||||||
20268|Winton Formation|40220|6|Mentioned|p7|||||||||
20268|Winton Formation|40249|6|Mentioned|p41|||||||||
20268|Winton Formation|40322|6|Mentioned|Fig.3|||||||||
20268|Winton Formation|40670|6|Mentioned|Fig.9|||||||||
20268|Winton Formation|40675|6|Mentioned|Table 8A|||||||||
20268|Winton Formation|40681|6|Mentioned|Fig.2|||||||||
20268|Winton Formation|40756|6|Mentioned|Fig.1.2|||||||||
20268|Winton Formation|40757|6|Mentioned|p78|||Now known to be Eyre Formation||||||
20268|Winton Formation|40801|6|Mentioned|p29|||Mention also Fig.21||||||
20268|Winton Formation|40910|6|Mentioned|p15|||See also P17||||||
20268|Winton Formation|40911|6|Mentioned|Map legend|Cenomanian|Albian|Albian-?Cenomanian||||||
20268|Winton Formation|40925|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
20268|Winton Formation|40926|3|Fully described|p18|||||||||
20268|Winton Formation|41057|6|Mentioned|p82|||||||||
20268|Winton Formation|41060|6|Mentioned|p3|||Generalized stratigraphy||||||
20268|Winton Formation|41061|6|Mentioned|p19|||||||||
20268|Winton Formation|41062|6|Mentioned|p35|||||||||
20268|Winton Formation|41063|6|Mentioned|p40|||||||||
20268|Winton Formation|41064|6|Mentioned|p62|||||||||
20268|Winton Formation|41085|6|Mentioned|p90|||||||||
20268|Winton Formation|41086|3|Fully described|p98|||See also Fig.3||||||
20268|Winton Formation|41088|6|Mentioned|p144|||See also Fig.2||||||
20268|Winton Formation|41097|6|Mentioned|Table 1|||||||||
20268|Winton Formation|41098|4|Described|p177|||||||||
20268|Winton Formation|41099|6|Mentioned|Fig.9|||||||||
20268|Winton Formation|41165|5|Briefly described|p363|||See also Fig.15.||||||19-DEC-06
20268|Winton Formation|41174|6|Mentioned|p117|||||||||
20268|Winton Formation|41176|6|Mentioned|p206|||See also P211||||||
20268|Winton Formation|41177|6|Mentioned|p233|||||||||
20268|Winton Formation|41182|5|Briefly described|Fig.2|||||||||
20268|Winton Formation|41183|4|Described|p307|||||||||
20268|Winton Formation|41184|6|Mentioned|p346|||||||||
20268|Winton Formation|41187|6|Mentioned|Fig.2|||||||||
20268|Winton Formation|41198|6|Mentioned|Table 1|||||||||
20268|Winton Formation|41214|6|Mentioned|Fig.3|||||||||
20268|Winton Formation|41216|6|Mentioned|p299|||||||||
20268|Winton Formation|41219|6|Mentioned|p338|||||||||
20268|Winton Formation|41266|6|Mentioned|Fig.3|||||||||
20268|Winton Formation|41523|3|Fully described|p282|||See also p283.||||||19-DEC-06
20268|Winton Formation|41535|6|Mentioned|p369|||||||||
20268|Winton Formation|41707|6|Mentioned|Fig.8|||||||||
20268|Winton Formation|41720|6|Mentioned|p372|||||||||
20268|Winton Formation|41724|5|Briefly described|p383|||||||||
20268|Winton Formation|41950|5|Briefly described|Fig.2 P3|||||||||
20268|Winton Formation|42061|4|Described|Fig,11 P159|||See also Fig.11||||||
20268|Winton Formation|42067|6|Mentioned|Fig.2 P309|||||||||
20268|Winton Formation|42071|6|Mentioned|p117|||||||||
20268|Winton Formation|42084|6|Mentioned|Fig.3 P256|||||||||
20268|Winton Formation|42085|6|Mentioned|Fig.2 P374|||||||||
20268|Winton Formation|42187|6|Mentioned|Fig.5 P322|||||||||
20268|Winton Formation|42293|6|Mentioned|Fig.2 P.18|||||||||
20268|Winton Formation|42346|5|Briefly described|p84|Cretaceous||||||||
20268|Winton Formation|42375|6|Mentioned|p30, p121, p125|Late Cretaceous|Jurassic|Eromanga Basin.||||||
20268|Winton Formation|42395|5|Briefly described|Fig.13 P83|||||||||
20268|Winton Formation|42397|6|Mentioned|Fig.2 P3|||||||||
20268|Winton Formation|42429|5|Briefly described|p155|Cenomanian||||||||
20268|Winton Formation|42447|6|Mentioned|Fig. 1|||||||||
20268|Winton Formation|42496|5|Briefly described|p136, Fig.3 p132|||||||||
20268|Winton Formation|42520|5|Briefly described|p6|||||||||
20268|Winton Formation|42543|5|Briefly described|Fig.4 P6|||||||||
20268|Winton Formation|42645|6|Mentioned|p195|||||||||
20268|Winton Formation|42648|5|Briefly described|Fig.7 P43|||||||||
20268|Winton Formation|42673|5|Briefly described|Fig.2, P184|||||||||
20268|Winton Formation|42746|4|Described|p12|||See also Fig.2, Fig.6||||||
20268|Winton Formation|42749|6|Mentioned|Fig.2 P27|||||||||
20268|Winton Formation|42784|6|Mentioned|p492|||||||||
20268|Winton Formation|42905|5|Briefly described|p20, Fig 5.3|||||||||
20268|Winton Formation|42999|5|Briefly described|Table 2,p90||Late Cretaceous|||||||
20268|Winton Formation|43002|5|Briefly described|Fig.2,p135|||||||||
20268|Winton Formation|43004|5|Briefly described|Table 1,p179|||||||||
20268|Winton Formation|43053|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Fluviolaustrine mudstone and siltstone.||||||25-MAY-05
20268|Winton Formation|43085|5|Briefly described|Fig.3|||||||||
20268|Winton Formation|43105|6|Mentioned|p15|||||||||
20268|Winton Formation|43114|6|Mentioned|Table 2|||||||||
20268|Winton Formation|43122|5|Briefly described|Fig.2.|||||||||
20268|Winton Formation|43252|5|Briefly described|p163|||||||||
20268|Winton Formation|43258|5|Briefly described|Map Legend||Cretaceous|||||||
20268|Winton Formation|43298|5|Briefly described|Map Legend||Cretaceous|||||||
20268|Winton Formation|43344|14|Not recorded|p14|||||||||
20268|Winton Formation|43383|14|Not recorded|p27|||||||||
20268|Winton Formation|43384|14|Not recorded|Map Legend||Cretaceous|||||||
20268|Winton Formation|43390|14|Not recorded|p16|||Part of Rolling Downs Group||||||
20268|Winton Formation|43452|14|Not recorded|Map Legend||Cretaceous|Of the Rolling Downs Group.||||||14-FEB-05
20268|Winton Formation|43459|14|Not recorded|p315|||||||||
20268|Winton Formation|43591|6|Mentioned|p40|||||||||
20268|Winton Formation|43602|6|Mentioned|191|||In Eromanga Basin, Rolling Downs Group||||||
20268|Winton Formation|43628|6|Mentioned|Fig.3|Late Cretaceous|Early Cretaceous|||||||
20268|Winton Formation|43883|14|Not recorded|p18 Fig.4-3|||||||||
20268|Winton Formation|43985|14|Not recorded|7-10,12,Fig.3,Pl.1,2|||||||||
20268|Winton Formation|43995|14|Not recorded|Tb.p9,30,57-8,Fig.3||Late Cretaceous|Fig.15||||||
20268|Winton Formation|44016|14|Not recorded|Map Legend|Late Cretaceous|Early Cretaceous|||||||
20268|Winton Formation|44017|14|Not recorded|Map Legend|||||||||
20268|Winton Formation|44018|14|Not recorded|Map Legend|Late Cretaceous|Early Cretaceous|||||||
20268|Winton Formation|44019|14|Not recorded|Map Legend|Late Cretaceous|Early Cretaceous|||||||
20268|Winton Formation|44020|14|Not recorded|p8,10-11,13-15,Tb.1,|Late Cretaceous|Early Cretaceous|Of Rolling Downs Group. Tb.2,3, Fig.3,||||||
20268|Winton Formation|44031|14|Not recorded|p5,6,8,9||Cretaceous|||||||
20268|Winton Formation|44033|4|Described|map,4,8,9,Tb.1|Late Cretaceous|Early Cretaceous|||||||
20268|Winton Formation|44034|4|Described|Tb.1,p2,4-6,9,10|||||||||
20268|Winton Formation|44040|14|Not recorded|p35|||||||||
20268|Winton Formation|44041|6|Mentioned|p251|||||||||
20268|Winton Formation|44066|14|Not recorded|Map Legend||Cretaceous|||||||
20268|Winton Formation|44067|14|Not recorded|Map Legend|Late Cretaceous|Early Cretaceous|||||||
20268|Winton Formation|44068|14|Not recorded|p17,18|||||||||
20268|Winton Formation|44082|14|Not recorded|p28,30,Tb.p34|||||||||
20268|Winton Formation|44087|14|Not recorded|p4,8-12|||Lacustrine.||||||
20268|Winton Formation|44088|14|Not recorded|Tb.1,opp.p6,7,8,map|||||||||
20268|Winton Formation|44089|4|Described|p3-6,8-10,Tb.1|Late Cretaceous|Early Cretaceous|||||||
20268|Winton Formation|44090|14|Not recorded|Map Legend|Late Cretaceous|Early Cretaceous|||||||
20268|Winton Formation|44091|14|Not recorded|p61||Cretaceous|||||||
20268|Winton Formation|44098|14|Not recorded|p98|||||||||
20268|Winton Formation|44099|14|Not recorded|Map Legend|Late Cretaceous|Early Cretaceous|(Rolling Downs Group)||||||
20268|Winton Formation|44115|14|Not recorded|p17,20|||||||||
20268|Winton Formation|44119|14|Not recorded|Map Legend||Cretaceous|||||||
20268|Winton Formation|44120|14|Not recorded|Map Legend||Cretaceous|||||||
20268|Winton Formation|44121|14|Not recorded|p5-8,10,12||Cretaceous|See also Lexicon.||||||
20268|Winton Formation|44122|2|Defined|p318-324|||||||||
20268|Winton Formation|44133|4|Described|p123, 104 Fig. 9.11|Cretaceous|Cretaceous|Geological Province: Eromanga Basin. Maximum Thickness: ~1200m. Includes part of the now superseded Blanchewater Formation.||||||
20268|Winton Formation|44168|14|Not recorded|Tb.1p5,7,8,10,map|||||||||
20268|Winton Formation|44269|14|Not recorded|p18||Cretaceous|||||||
20268|Winton Formation|44291|14|Not recorded|p5|||||||||
20268|Winton Formation|44310|14|Not recorded|Map Legend||Cretaceous|||||||
20268|Winton Formation|44346|14|Not recorded|p4|||||||||
20268|Winton Formation|44374|14|Not recorded|p12||Cretaceous|Freshwater-final withdrawal of sea from Eromanga Basin.||||||
20268|Winton Formation|44375|14|Not recorded|p313|||||||||
20268|Winton Formation|44405|14|Not recorded|Map Legend|Late Cretaceous|Early Cretaceous|||||||
20268|Winton Formation|44406|14|Not recorded|p3-14|Cenomanian|Albian|||||||
20268|Winton Formation|44407|14|Not recorded|Map Legend|||||||||
20268|Winton Formation|44408|14|Not recorded|p4,8-13,opp.6|||||||||
20268|Winton Formation|44410|14|Not recorded|Map Legend|Late Cretaceous|Early Cretaceous|||||||
20268|Winton Formation|44413|14|Not recorded|p470,474|||||||||
20268|Winton Formation|44414|14|Not recorded|p110-112||Cretaceous|Mudstone, siltstone and characteristic coal seams.||||||
20268|Winton Formation|44415|14|Not recorded|p22|||||||||
20268|Winton Formation|44417|14|Not recorded|p416,417,420|||||||||
20268|Winton Formation|44418|14|Not recorded|Map Legend|Late Cretaceous|Early Cretaceous|||||||
20268|Winton Formation|44509|14|Not recorded|p342-343|||||||||
20268|Winton Formation|44548|14|Not recorded|p456||Cretaceous|||||||
20268|Winton Formation|44573|14|Not recorded|p98|||||||||
20268|Winton Formation|44611|14|Not recorded|p22,24|||||||||
20268|Winton Formation|44634|14|Not recorded|p29|||||||||
20268|Winton Formation|44715|14|Not recorded|Map Legend|||||||||
20268|Winton Formation|44732|14|Not recorded|Pl.1|||Taken from GeolMap QLD 1953.||||||
20268|Winton Formation|44807|14|Not recorded|p10|||||||||
20268|Winton Formation|44819|14|Not recorded|p89,90|||Non-marine sandstone, carbonaceous grey shale and coal. No age given.||||||
20268|Winton Formation|44848|14|Not recorded|p99-101|||||||||
20268|Winton Formation|44852|14|Not recorded|p78||Late Cretaceous|||||||
20268|Winton Formation|44915|14|Not recorded|p18,24|||Correlated with upper part of Blanchewater Formation in South Australia. Age not given.||||||
20268|Winton Formation|44998|14|Not recorded|p.169|||||||||
20268|Winton Formation|45004|14|Not recorded|p.8,9|||||||||
20268|Winton Formation|45110|6|Mentioned|Table 18|||||||||
20268|Winton Formation|45168|6|Mentioned|p6|||See also Table 1||||||
20268|Winton Formation|46791|5|Briefly described|p48|||||||||
20268|Winton Formation|46854|6|Mentioned|p241|||||||||
20268|Winton Formation|46911|5|Briefly described|p112|||Analyses of weathered profiles and parent rocks.||||||
20268|Winton Formation|46937|5|Briefly described|Fig.10|||See also Table 1.||||||
20268|Winton Formation|46939|6|Mentioned|Fig.1|||See also Table 1.||||||
20268|Winton Formation|48627|14|Not recorded|p3|||||||||
20268|Winton Formation|48634|4|Described|p5,19,20|||See also Fig.2,6,Pl.1,2. Subsidy report. (G54-14).||||||
20268|Winton Formation|48751|6|Mentioned|p19|||||||||
20268|Winton Formation|48906|14|Not recorded|p5,9,Tb.2,Fig.1,Pl.1|Late Cretaceous|Early Cretaceous|||||||
20268|Winton Formation|48908|14|Not recorded|Tb.1||Late Cretaceous|||||||
20268|Winton Formation|48920|3|Fully described|p62|||Cretaceous age||||||
20268|Winton Formation|49010|6|Mentioned|Fig.4|||Eromanga Basin||||||
20268|Winton Formation|49011|6|Mentioned|Fig.3|||In the Eromanga Basin.||||||19-DEC-06
20268|Winton Formation|60080|5|Briefly described|Map legend|Late Cretaceous|Early Cretaceous|Very labile sandstone, siltstone and mudstone; calcareous in part, minor mud clast conglomerate.  Overlain by Glendower Formation.||||||22-JUL-04
20268|Winton Formation|60281|6|Mentioned|p11|||||||||
20268|Winton Formation|60331|5|Briefly described|p34 Fig.3||Cenomanian|Overlies Mackunda Formation. Geological Province: Eromanga Basin||||||
20268|Winton Formation|60717|5|Briefly described|p40 Fig. 2|Late Cretaceous|Late Cretaceous|Overlies Oodnadatta Formation and Mackunda Formation. Geological Province: Eromanga Basin. Non-marine to marginal marine deposits.||||||31-JAN-08
20268|Winton Formation|60726|6|Mentioned|p2 Fig.1, p6.|Late Cretaceous|Late Cretaceous|Winton area, Great Artesian Basin.||||||
20268|Winton Formation|60953|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Fluviolacustrine mudstone and siltstone.||||||
20268|Winton Formation|61108|5|Briefly described|map legend|Cretaceous|Cretaceous|Fluviolacustraine mudstone and siltstone.||||||
20268|Winton Formation|61312|5|Briefly described|p75, p79 Table E2|Cretaceous|Cretaceous|Of the Rolling Downs Group. Consists of interbedded mudstone and lithic and feldspathic sandstone deposited in terrestrial environments. Geological Province: Eromanga Basin (absent in NSW). See also p64, p67 Fig. E5.||||||19-DEC-06
20268|Winton Formation|61611|6|Mentioned|p265 Fig. 3|Early Cretaceous|Early Cretaceous|Geological Province: Eromanga Basin.||||||13-MAR-09
20268|Winton Formation|61613|6|Mentioned|p282 Fig. 2|Late Cretaceous|Late Cretaceous|Geological Province: Eromanga Basin.||||||07-FEB-11
20268|Winton Formation|61614|6|Mentioned|p290 Fig. 2|Late Cretaceous|Early Cretaceous|Geological Province: Eromanga Basin.||||||17-MAR-09
20268|Winton Formation|61823|5|Briefly described|p118|Cenomanian|Late Albian|Predominantly alluvial deposits.  Geological Province: Eromanga Basin.||||||
20268|Winton Formation|62028|5|Briefly described|p10 Fig. 1|||||||||
20268|Winton Formation|62029|5|Briefly described|p15 Fig. 4|Cretaceous|Cretaceous|||||||
20268|Winton Formation|62046|5|Briefly described|p125 Fig. 2|Cretaceous|Cretaceous|Geological Province: Cooper-Eromanga Basins.||||||14-APR-08
20268|Winton Formation|62376|5|Briefly described|p84|Late Cretaceous|Early Cretaceous|Geological Province: Pedirka Basin.||||||09-FEB-10
20268|Winton Formation|62537|6|Mentioned|p191 Fig.2. |Late Cretaceous|Late Cretaceous|Eromanga Basin.||||Overlies Mackunda Formation.||
20268|Winton Formation|62730|5|Briefly described|p352 Fig. 1|Late Cretaceous|Late Cretaceous|Geological Province: Eromanga Basin.||||||21-APR-08
20268|Winton Formation|63979|2|Defined|p54-55, Fig. 44|Cenomanian|Albian|Formerly Winton Series (Dunstan 1916). Forms upper part of Rolling Downs Gp.Conformable on Mackunda Fm; unconformable below Glendower Fm. Max.thick:1000m. Interbedded sands., sandy siltst., siltst., mudst.+ coal with minor intraformational conglomerate.||||||07-FEB-11
20268|Winton Formation|64048|5|Briefly described|p64 Tb. 2|||Source of hydrocarbons - lignite. Geological Province: Eromanga Basin.||||||07-FEB-11
20268|Winton Formation|64197|6|Mentioned|p625 Fig.1c, p627, p630 Figs.6,7|Late Cretaceous|Late Cretaceous|Eromanga Basin. Deeply weathered upper surface.||||Overlies Oodnadatta and Mackunda Formations. Is overlain unconformably by Eyre Formation.||11-DEC-15
20268|Winton Formation|64232|5|Briefly described|p12|Cretaceous|Cretaceous|Geological Province: Eromanga Basin. Coal measures are present in this unit and are a potential target for CSM exploration activities.||||||24-JUL-08
20268|Winton Formation|64665|5|Briefly described|p62.|Cretaceous|Cretaceous|Eromanga Basin. Hosts coal seams up to 7 m thick; low rank lignites of no current (i.e. c.2008) commercial interest.||||||
20268|Winton Formation|64778|6|Mentioned|p13|Cretaceous|Cretaceous|Pedirka and Simpson Desert Basins.||||||
20268|Winton Formation|64856|6|Mentioned|p101|||Eromanga Basin. Younger than lithologically similar Griman Creek Formation in the Surat Basin.|| ||||29-NOV-17
20268|Winton Formation|65238|5|Briefly described|p7 Fig. 8, p10|Early Cretaceous|Early Cretaceous|Geological province: Eromanga Basin. Fluvial deposits.||||||
20268|Winton Formation|65342|5|Briefly described|p9.|||Eromanga Basin. Max. thickness at least 613 m. Seen as having potential as an insulating layer for geothermal energy.||||Overlies Oodnadatta Shale. Is overlain by Eyre Formation.|Sandstone, siltstone, mudstone; minor conglomerate, coal; predominantly alluvial deposits.|
20268|Winton Formation|65376|5|Briefly described|p9 Fig.1.2. |Cretaceous|Cretaceous||||||Marginal marine to fluvial mudstone and siltstone.|
20268|Winton Formation|65385|5|Briefly described|pS134 Fig.7|Late Cretaceous|Early Cretaceous|Of Eromanga Basin. Overlies Mackunda Formation.||||||08-MAR-12
20268|Winton Formation|65489|5|Briefly described|p49, p53, p55, p57-61, p96, p155-156|Late Cretaceous|Late Cretaceous|Eromanga Basin. 1200m thick. Rapid non-marine deposition: c.1100m in c.8 m.y.||||Overlies Mackunda and Oodnadatta Formations. Is locally overlain unconformably by Mount Howie Sandstone.||
20268|Winton Formation|65925|5|Briefly described|p15, Appendix 2.|||Thousand-metre thick package deposited in low-energy fluvial to lacustrine environment.|||||Sandstone, shale, siltstone; coal seams.|
20268|Winton Formation|66131|6|Mentioned|p239|Cenomanian|Cenomanian|||||||
20268|Winton Formation|66529|5|Briefly described|p10, p12 Fig.5 |||Eromanga Basin.||Unit in Rolling Downs Group.||Overlies Mackunda and Normanton Formations.|~1000m thick package of non-marine sandstones, shales and siltstones.|
20268|Winton Formation|66623|3|Fully described|p242, p245, pp256-257, pp266-267.|Cenomanian|Albian|Marks the stratigraphic top of the Rolling Downs Group throughout the Eromanga Basin. Correlates with upper half of Yalpunga Beds. Very poor outcrop; extensive post-deposition erosion reduced thickness from 0 to 1100 m. Fossils include vertebrates, plants, wood and microfossils.||Unit in Rolling Downs Group.||Conformably overlies Allaru Mudstone. Is overlain unconformably by fluvial Paleogene sedimentary rocks of Lake Eyre Basin, and by Cordillo Silcrete capping.|Medium-grained, cross-bedded sandstone with rounded intraclasts of siltstone and mudstone; calcareous labile sandstone, siltstone, carbonaceous and pyritic shale with intraclast conglomerate and minor coal; fresh volcanic detritus in sandstones.|07-JUN-13
20268|Winton Formation|66915|5|Briefly described|p6 Fig.3|Cretaceous|Cretaceous|Eromanga Basin.||||||
20268|Winton Formation|67119|5|Briefly described|Map legend.|Cretaceous|Cretaceous|Non-marine.|||||Shale, siltstone, sandstone; minor coal horizons.|
20268|Winton Formation|67323|5|Briefly described|p86-87, p92, p93 Fig.12.3, p95 Fig.12.5|Cretaceous|Cretaceous|See also GIS attrib tbl, Solid Geology Map. Eromanga/Carpentaria Basins. Oil shale was discovered in two wells (AAP Fermoy 1 and AAP Mayneside 1) in this unit by Australian Aquitaine Petroleum Pty Ltd in 1966. Attention shifted to outcrops in Julia Creek but activity ceased in 1969. Fluvial deposits. Underwent deep chemical weathering during Late Cretaceous to Palaeogene.||||Overlies Mackunda Formation.|Labile sandstone, siltstone, mudstone, minor coal.|
20268|Winton Formation|67402|4|Described|p26 tbl RRM4|Cenomanian|Cenomanian|Eromanga Basin. Maximum thickness of 1000m. Deposited in fluvial and lacustrine environments. Estimated porosity of 10-25% with likely favourable permeability for Carbon dioxide storage. See also p106, p108, p109, p111 fig ERO8, p115 tbl ERO2.||||Overlies the Mackunda Formation.|Interbedded sandstone, sandy siltstone, siltstone, mudstone and coal with minor intraformational conglomerate.|
20268|Winton Formation|67462|5|Briefly described|Map legend.|Late Cretaceous|Late Cretaceous|Eromanga Basin.||||Overlies Oodnadatta Formation.||
20268|Winton Formation|67578|6|Mentioned|p335 Fig.2|Cretaceous|Cretaceous|Lake Eyre region.||||||
20268|Winton Formation|67784|5|Briefly described|p25, p31|Cenomanian|Albian|Northern Eromanga Basin. Up to 400m thick. Non-marine deposits.||||Overlies Mackunda Formation||08-FEB-18
20268|Winton Formation|68003|5|Briefly described|p63 Fig.3-p.|Cretaceous|Cretaceous|Surat Basin.||||Overlies Coreena Member.||
20268|Winton Formation|68004|6|Mentioned|p204.|||Hosts opal. Ferruginisation increases toward the basal one-third of the profile.||||||
20268|Winton Formation|68068|5|Briefly described|Map legend|Cenomanian|Cenomanian|Eromanga Basin. Subsurface only. Fluvial to paludal-lacustrine. Fossil wood and leaves, freshwater bivalves, fish and vertebrates.||Unit in Neales River Group.||Conformably and gradationally overlies Mackunda Formation.|Dark grey-brown sandy silt-clay, finely laminated and cross-bedded, weakly bioturbated; basal portions carbonaceous to lignitic: lowest coal often taken as base of unit.|
20268|Winton Formation|68131|5|Briefly described|p2 Fig.1|Cretaceous|Cretaceous|Marginal marine to fluvial sediments. Mapped with Winton Formation as one unit.|||||Mudstone and siltstone.|
20268|Winton Formation|68206|6|Mentioned|p28|Cenomanian|Cenomanian|Great Artesian Basin. Marks a return to non-marine conditions after Barremian-Albian inundation.||||||
20268|Winton Formation|68553|6|Mentioned|Map legend; schematic diagram.|Cretaceous|Cretaceous|Eromanga and Carpentaria Basins.||Unit in Rolling Downs Group.||Conformably overlies Mackunda Formation.||
20268|Winton Formation|68713|5|Briefly described|p22|Cretaceous|Cretaceous|||Of the Neales River Group.||||
20268|Winton Formation|68715|6|Mentioned|p30 Fig.5|Cenomanian|Albian|Eromanga Basin.||||||
20268|Winton Formation|68731|6|Mentioned|pp209-211|||||||||
20268|Winton Formation|68734|5|Briefly described|p218 Fig.2, p218, p221 Fig.3|Cenomanian|Albian|Eromanga Basin (SW and NE). Fluvial to lacustrine. Late Albian maximum age. Opal is typically found in the upper 1-2 m of a claystone layer underlying a sandstone layer.||Of the Rolling Downs Group.|||Volcaniclastic.|18-JAN-22
20268|Winton Formation|68821|4|Described|p292 Fig.1, pp294-302, p307, p308 Fig.10|Cenomanian|Albian|Late Albian Maximum age. Contains ubiquitous disseminated pyrite. Preserved thickness is approximately 1200 m in the centre of the Eyre Basin. Fluvial to fluvial-lacustrine depositional environment.|97 - 93 Ma|Of the Rolling Downs Group.||Unconformably overlain by the Eyre Formation.|Comprises fluvial sandstone and siltstone.|
20268|Winton Formation|68901|5|Briefly described|p7 Fig. ii|||Eromanga Basin.||Rolling Downs Group|||Sandstone, siltstone, mudstone, calcareous in part.|27-SEP-18
20268|Winton Formation|69001|6|Mentioned|p18|Late Cretaceous||||||||
20268|Winton Formation|69019|4|Described|p83 Fig.20,p85,p94 Fig.24,p100-103,p169|Turonian|Cenomanian|Of Whitehouse (1953); formerly Winton Series (Dunstan, 1916). Named after Winton, Qld. Terrestrial deposition. Thickness from 0-150 m. Contains fossils of plants, lungfish teeth and possible dinosaur bone fragments. Of interest to explorers for biogenic coal seam gas.||Unit in Neales River Group.||Overlies Mackunda Formation. Is overlain disconformably by Eyre Formation and locally by Mount Howie Sandstone.|Dark khaki-grey to dark grey-brown, carbonaceous and pyritic mudstone interbedded with pale grey, fine-grained calcareous sandstone, sometimes feldspathic; seams of coal or lignite at/near the base; abundant plant fossils.|
20268|Winton Formation|69023|5|Briefly described|p79, p86-87, p89 Fig.20, p93, p100|Turonian|Cenomanian|See also p105-106, p110, p112, p163, p191-192. Whitehouse (1955); formerly the Winton Series of Dunstan (1916) for freshwater sediments with coal seams in bores around Winton, Qld. Eromanga Basin. Resembles underlying Mackunda Formation. <40m thick. Contains plant, invertebrate and vertebrate fossils. Stratigraphic wells intersection data.||||Conformably overlies Mackunda Formation and Marree Subgroup. Is overlain disconformably by Eyre Formation.|Dark khaki-grey to grey, carbonaceous and pyritic mudstone interbedded with pale grey, fine-grained, calcareous sandstone and coal seams. Typically weathers to yellow or white kaolinitic sandstone.|
20268|Winton Formation|69454|5|Briefly described|p38:3, 13|Late Cretaceous|Late Cretaceous|Eromanga Basin. Deposition of this thick unit initiated hydrocarbon generation in underlying Permian and post-Permian source rocks.||||||12-JUL-16
20268|Winton Formation|69457|3|Fully described|p41:2-6, 9, 11-13, 17|Late Cretaceous|Early Cretaceous|Whitehouse (1955). Uppermost unit in the Eromanga Basin. Formerly part of the superseded Blanchewater Formation, used for the combined undifferentiated Mackunda-Winton Formations interval. Fluviatile to paludal to lacustrine deposits; paralic, estuarine, deltaic and fluviatile near base. Maximum 620m thick in NT; c.1200m in the Patchawarra Trough in SA. Poorly exposed as highly weathered outcrops around dry lakes. Contains abundant micro- and macroflora and macrofauna. Late Albian to early Cenomanian. The seams of brown to black coal are uneconomic. Sediment loading by this thick unit is believed to have triggered hydrocarbon generation.||Manuka Subgroup.||Conformably overlies Mackunda Formation.|Claystone, siltstone and mudstone with interbedded very fine- to medium-bedded sandstone, and minor coal seams usually interbedded with carbonaceous mudstone; local minor intraformational conglomerate. Contains plant fragments and fossil wood.|12-JUL-16
20268|Winton Formation|69555|5|Briefly described|p43-44, p46-48|Turonian|Albian|Comprises the youngest Cretaceous strata of the Eromanga Basin. Fossil flora (palynological and macro) listed and described.||Rolling Downs Group|||Fossiliferous fine- to medium-grained, feldspatholithic or lithofeldspathic arenites, siltstones, mudstones and claystones, with very minor coal seams.|13-FEB-18
20268|Winton Formation|69582|6|Mentioned|p65|Late Cretaceous|Late Cretaceous|Eromanga Basin.||||Overlies the Mackunda Formation.||
20268|Winton Formation|69594|5|Briefly described|p519, p526, p530-532, p563, p574|Cenomanian|Albian|Whitehouse (1955); Gray et al. (2002). Youngest deposits in the Eromanga Basin. Up to 1000m thick. The Mackunda-Winton boundary is difficult to pick. Unweathered outcrop is mainly well-cemented nodular sandstone; weathered outcrop is kaolinitised and ferruginised sandstones, mudstones and siltstone. Paralic, estuarine, deltaic and fluvial deposits in lower part; fluvio-lacustrine higher up. Contains a rich and diverse fossil flora, fauna and ichnofauna (listed and photographs); supports an economically important tourism industry. Detrital zircon plot.|~95 Ma (detrital zircon MDA: Greentree 2011).|||Conformably overlies Mackunda Formation.|Interbedded labile volcanic lithic-crystal sandstone, sandy siltstone, siltstone, mudstone, intraformational conglomerate and coal. Much of the detritus is volcanogenic.|
20268|Winton Formation|69599|5|Briefly described|p599-600|Cretaceous|Cretaceous|||||Is overlain unconformably by Old Cork beds, Moses Sandstone, Edkins and Glendower Formations.||
20268|Winton Formation|69673|4|Described|p155 fig 127|Cretaceous|Cretaceous|Up to 620m thick.||Manuka Subgroup||Overlies Mackunda Formation, overlain by Mount Howie Sandstone Member|Claystone, siltstone and mudstone with interbedded very fine to fine to occasionally medium grained sandstone and minor coal seams.|
20268|Winton Formation|69742|5|Briefly described|p787, 788, 790, 793|Cenomanian|Albian|Great Artesian Basin. Hosts opal. Fluvial volcaniclastics. Geochemistry discussed.|||||Red-brown ironstone dominated by goethite and kaolinite with minor quartz and illite.|
20268|Winton Formation|69751|6|Mentioned|p35-38, 41|Cretaceous|Cretaceous|Eromanga Basin. Freshwater, broad fluvial-lacustrine environment of deposition (at least the upper part). Contains rich fossil assemblages; also silicified wood. Cenomanian-Turonian climate was seasonal and variable, with potential flooding and/or drought.|||||Fine- to medium-grained feldspatholithic or lithofeldspathic arenites, siltstones, mudstones and claystones; very minor coal seams.|
20268|Winton Formation|69797|5|Briefly described|p17 Fig.2|Late Cretaceous|Late Cretaceous|Geol. Prov: Eromanga Basin.||||||
20268|Winton Formation|69946|2|Defined|p27-28, p56-57, p124-125, p129|Late Cretaceous|Late Cretaceous|Eromanga Basin. Originally Winton Series (Dunstan, 1916), without formal definition. Renamed Winton Formation by Whitehouse (1955). His type section is 'blue shales and sandstones with intercalated coal seams met within the bores in and around Winton'. Distinguishing from Mackunda Formation is difficult in SA due to lack of coals, but easier in Qld due to coal seams, intraformational conglomerates and absence of marine fossils. 400-1100m thick. Late Albian - Cenomanian. Freshwater fossils listed. The top has been deeply (>40m) weathered.||||Conformably overlies Mackunda Formation. Is overlain unconformably by Eyre Formation.|Interbedded fine- to coarse-grained sandstone, carbonaceous and pyritic shale, siltstone and coal seams with intraclast conglomerates. Sandstone beds contain abundant fresh volcanogenic debris, lithics and feldspar.|
20268|Winton Formation|69947|5|Briefly described|p3, p9, p13 Fig.7.2|Late Cretaceous|Late Cretaceous|The final deposits in the Eromanga Basin. Is overlain by Tertiary sediments of the Lake Eyre Basin. On p9 the authors state: "the fluviolacustrine Winton Formation of the upper Marree Subgroup", which contradicts what appears in Fig.7.2.||||||
20268|Winton Formation|69948|6|Mentioned|p6; Figs.4.1, 18|||Eromanga Basin. Surface exposures of this and older units define the Birdsville Track Ridge.||||Overlies Mackunda Formation.||
20268|Winton Formation|69952|5|Briefly described|p16|Cretaceous|Cretaceous|Eromanga Basin.||Unit in Rolling Downs Group.|||Sandstone, siltstone, mudstone; calcareous in part.|
20268|Winton Formation|70383|5|Briefly described|p45|Cretaceous|Cretaceous|Eromanga Basin. Non-marine deposits.||||||
20268|Winton Formation|70649|5|Briefly described|Map Legend|Cretaceous|Cretaceous|||Rolling Downs Group|||Non-marine mudstone and siltstone with subordinate interbedded coarse lithic and feldspathic labile sandstone.|18-JAN-22
20268|Winton Formation|70720|6|Mentioned|p6|||Eromanga Basin.||||Overlies Coreena Member. Is overlain by Glendower Formation.||
20268|Winton Formation|70789|5|Briefly described|p318, p320 Fig.4|Cenomanian|Cenomanian|Eromanga Basin.|c.93 Ma.||||Marine mudstones, siltstones and shales.|
20268|Winton Formation|70821|4|Described|p21-24, p30-31, p33, p79-80, p82|Late Cretaceous|Late Cretaceous|See also p85-87, p115-116. Youngest Formation in the Eromanga Basin. Much of this unit in the southern Thomson region has been removed by erosion. Crops out as low breakaways, intensely weathered (kaolinitised and ferruginised): the weathering profile can be up to 95m deep. One of the two main groundwater resources in the Great Artesian Basin. Paralic, estuarine, deltaic and fluvial deposits in the lower part; fluvio-lacustrine in the upper. Fossil biota is dominated by fish, crocodiles, dinosaurs and pterosaurs. Late Albian to Cenomanian. Hydrochemistry mentioned; hydrostratigraphic properties.||Rolling Downs Group.||Overlies Mackunda Formation and locally the Wallumbilla Formation (conformably). Is overlain unconformably by Glendower Formation.|Interbedded labile volcanic lithic-crystal sandstone, sandy siltstone, siltstone, mudstone, intraformational conglomerate and coal. Also pyritic black shale. Much of the clastic material is volcanogenic, presumably from volcanic arcs to the E.|
20268|Winton Formation|70823|5|Briefly described|p25-p27, p41, p43-p45, p78|Cenomanian|Cenomanian|Eromanga Basin. Up to 1200m thick. Deposited in a non-marine to marginal marine environment. Hosts lignite source rock. Age range derived from Bryan et al., 2012 and Tucker et al., 2013.|c. 99-93 Ma|||Overlies the Mackunda and Oodnadatta Formations. Overlain by the Mount Howe Sandstone.||
20268|Winton Formation|70824|5|Briefly described|p9|Cretaceous|Cretaceous|Eromanga Basin. Hosts lignite.||||Overlies the Mackunda Formation.||
20268|Winton Formation|70836|6|Mentioned|p474, 482|Turonian|Albian|Eromanga Basin. Preserves a rich and diverse vertebrate fauna including the only named Australian megaraptoran, Australovenator.|c.103-92 Ma (Tucker et al., 2013).|||||
20268|Winton Formation|70938|5|Briefly described|p816|Late Cretaceous|Late Cretaceous|Extensive, fluvial deposits. Paleocurrents and detrital zircons indicate a NE Queensland source.|||||Contains extensive labile volcanic detritus.|
20268|Winton Formation|71251|4|Described|p8, p11-13, p15, p17-20, p29, p49|||Senior (1971). Eromanga Basin. 47m total thickness in Eulo 1 borehole. Non-marine deposits. Natural gamma, magnetic susceptibility data tabulated. Conductivity data/diagram.||||Overlies Coreena Member (Wallumbilla Formation).|Dark grey siltstone, weathering to white, finely-bedded mudstone and claystone mottled by goethite and hematite, with gypsum prevalent throughout the top of the unit; capped by a 5m-thick duricrust of porcellanite (white silicified mudstone).|
20268|Winton Formation|71321|5|Briefly described|p15,65|Cenomanian|Cenomanian|Of Eromanga Basin. Regressivee depositional package following peak early Cretaceous marine transgression; fluvio-lacustrine siltstone and sandstones and locally coal-bearing.||||Overlain by Mount Howie Formation. Underlain by Mackunda Formation.|Fluvio-lacustrine siltstone and sandstones and locally coal-bearing.|
20268|Winton Formation|71342|3|Fully described|Ch 1 p6, Ch 1 p19, Ch3 p4, Ch4 p6|Cenomanian|Albian|Eromanga Basin. Originally termed the Winton Series by Dunstan (1916) without formal definition. The name was changed to Winton Formation and a type section was designated in Queensland by Whitehouse (1955). The type section is described as "blue shales and sandstones with intercalated coal seams met within the bores in and around Winton". Hosts a major confined aquifer. Lithology, sedimentology, distribution and outcrop characteristics are discussed. This unit is generally thicker than 400m in the Cooper region and has a maximum thickness of 1100m in the northern Patchawarra Trough. Age derived on the basis of palynology and macrofossil assemblage. Spore-pollen zone is given in Ch5 p57. See also Ch4 p8, Ch4 p25, Ch5 p27-p28, Ch5 p30, Ch5 p33, Ch5 p56-p57, Ch5 p126-p127, Ch5 p130, Ch6 p9-p10, Ch7 p3, Ch7 p9, Ch7 p13, Ch9 p4-p5, Ch9 p10-p11, Ch9 p18, Ch10 p3.||||Conformably overlies the Mackunda Formation. Overlies the Oodnadatta Formation. Unconformably overlain by the Eyre Formation.|Interbedded fine to coarse-grained sandstone, carbonaceous and pyritic shale, siltstone and coal seams with intraclast conglomerates.|
20268|Winton Formation|71601|6|Mentioned|p120, p121|Turonian|Albian|Central west Qld. Ankylosaurian remains have been identified.||||||
20268|Winton Formation|71855|6|Mentioned|p20, p27, p30|||||||||
20268|Winton Formation|71863|5|Briefly described|p5|Cenomanian|Albian|Eromanga Basin.||||Overlies the Allaru Mudstone and the Mackunda Formation.||
20268|Winton Formation|71864|4|Described|p8, p10, p13-p14, p16-p20, p26|||Intersected in GSQ Eulo 2 borehole between 2-23m depth. Originally mapped in the area by Senior (1971). Described in Senior, 1971 as non-marine fine sandstone and siltstone. Gamma log characteristics and magnetic susceptibility is provided.||||Overlies the Wallumbilla Formation.|Mottled, deeply weathered mudstone regolith with gypsum flakes throughout, blue siltstone and thin quartzose and lithic gravel bands.|
20268|Winton Formation|72297|5|Briefly described|p700, p724, p751, p758|Cretaceous|Cretaceous|Eromanga Basin. All coal seams are of uneconomic thickness and of poor quality. CSG exploration results not encouraging. Has a large kaolin deposit 35km W of Winton (70-80% kaolinite). Hosts QLD's opal fields within a 300km wide, NNW-trending belt from Hungerford to Kyuna.|||||White mudstone. Contains seams of subhydrous lignite - sub-bituminous black coal.|
20268|Winton Formation|72298|5|Briefly described|p801|Cretaceous|Cretaceous|Eromanga Basin. Confined aquifers, generally producing non-flowing artesian water bores.||Rolling Downs Group.||Overlies Rumbalara Shale, Mackunda FZ.||
20268|Winton Formation|72456|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Marree 1:250k map sheet.|||||Shale, siltstone, sandstone that is non-marine with minor coal horizons.|
20268|Winton Formation|72915|6|Mentioned|p16|||Absent in the area of the Congararra 1 borehole (after Hawke and Cramsie, 1984).||||||
20268|Winton Formation|73106|5|Briefly described|Map legend.|Cretaceous|Cretaceous||||||Shale, siltstone, sandstone. Non-marine, minor coal horizons.|
20268|Winton Formation|73167|6|Mentioned|p664 Fig. 2|Cretaceous|Cretaceous|Eromanga Basin.||||||
20268|Winton Formation|73249|6|Mentioned|p319|Cretaceous|Cretaceous|Eromanga Basin.||||Overlies the Mackunda Formation.||
20268|Winton Formation|73251|6|Mentioned|p62|Late Cretaceous|Late Cretaceous|Eromanga Basin. Non-marine to marginal marine.||||Underlain by Mackunda Formation and Oodnadatta Formation.||
20268|Winton Formation|73281|6|Mentioned|Appendix (DIP)|||See DIP034_Petroleumdata.xlsx and DIP034_Welldata.xlsx.||||||
20268|Winton Formation|73343|6|Mentioned|p337|Cretaceous|Cretaceous|Eromanga Basin.||||Underlain by Oodnadatta Formation. Equivalent to Mackunda Formation.||
20268|Winton Formation|73393|6|Mentioned|p20||||||||Includes volcaniclastic sedimentary deposits.|
20268|Winton Formation|73479|5|Briefly described|p155, p156 Fig.2, p159-160|Cretaceous|Cretaceous|Eromanga Basin. Fluvial-lacustrine depositional environment. Significantly eroded following exhumation (late Cretaceous).|ca 97-93 Ma|||Overlies Oodnadatta Formation, unconformably underlies Eyre Formation||
20277|Winulta Formation|22643|5|Briefly described|p191, fig3|Early Cambrian|Early Cambrian|||||||
20277|Winulta Formation|22755|6|Mentioned|p555|||||||||
20277|Winulta Formation|22766|4|Described|Fig.2 p561,563||Tommotian|||||||
20277|Winulta Formation|23719|5|Briefly described|p26|Paleozoic|Paleozoic|Geological Province: Gawler Craton.||||||07-NOV-08
20277|Winulta Formation|23981|5|Briefly described|p8-9 Fig. 4, p20|Tommotian|Tommotian|Conformably overlain by Kulpura Formation. Max. thickness: 100m. Geol.Prov: Stansbury Basin. Conglomerate and flaggy sandstones in northern part of Yorke Pen. and thicker, finer-gr. with shelly fossils in southern part.||||||
20277|Winulta Formation|24360|5|Briefly described|p53|Cambrian|Cambrian|Geological Province: Yorke Peninsula, Gawler Craton||||||
20277|Winulta Formation|24465|5|Briefly described|p345 Fig.2|Early Cambrian|Early Cambrian|Geological Province: Stansbury Basin.||||||19-JAN-05
20277|Winulta Formation|24475|5|Briefly described|p56|Early Cambrian|Early Cambrian|Overlies both the Aagot Member and Curramulka Gabbronorite.||||||
20277|Winulta Formation|35255|6|Mentioned|Fig.8|||||||||
20277|Winulta Formation|36244|6|Mentioned|p2|||Refers Thomson et al.1976.||||||
20277|Winulta Formation|38873|6|Mentioned|p4|||||||||
20277|Winulta Formation|39349|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
20277|Winulta Formation|39352|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
20277|Winulta Formation|40852|6|Mentioned|p32|||||||||
20277|Winulta Formation|40856|6|Mentioned|Fig.23.6|||||||||
20277|Winulta Formation|41526|6|Mentioned|p61|||||||||
20277|Winulta Formation|42192|6|Mentioned|p10|||||||||
20277|Winulta Formation|42222|6|Mentioned|p20|||||||||
20277|Winulta Formation|42225|4|Described|p217|||||||||
20277|Winulta Formation|42235|5|Briefly described|p141|||||||||
20277|Winulta Formation|42271|6|Mentioned|p372|||||||||
20277|Winulta Formation|42488|5|Briefly described|Fig.2 P187|||||||||
20277|Winulta Formation|43052|5|Briefly described|Table 2.1|||||||||
20277|Winulta Formation|44133|5|Briefly described|p4 Fig. 7.2, 6, 7|Early Cambrian|Early Cambrian|Geological Province: Stansbury Basin. Discordantly overlies lower Wilpena Group.||||||03-MAY-13
20277|Winulta Formation|60953|5|Briefly described|Map Legend|Cambrian|Cambrian|Geological Province: Spencer Shelf.||||||
20277|Winulta Formation|60958|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Arkosic sandstone to quartzite with minor siltstone and basal conglomerate. Uppermost part is dolomitic and silty. Geological Province: Stansbury Basin.||||||14-APR-05
20277|Winulta Formation|61108|5|Briefly described|map legend|Cambrian|Cambrian|Marine shelf to basinal carbonate. Geological Province: Arrowie Basin.||||||
20277|Winulta Formation|61121|5|Briefly described|Map legend|Early Cambrian|Early Cambrian|Arkosic sandstone to quartzite with minor siltstone and basal conglomerate; dolomitic in upper section.  Age is Tommotian. Geological Province: Stansbury Basin.||||||06-JUN-05
20277|Winulta Formation|64282|5|Briefly described|Map legend|Early Cambrian|Early Cambrian|Geological Province: Stansbury Basin. Age is Tommotian. Arkosic sandstone to quartzite with minor siltstone and basal conglomerate; uppermost part is dolomitic and silty. Contains Hyolithids, trace fossils.||||||24-JUL-08
20277|Winulta Formation|65375|4|Described|pp25-28, p40, p53.|Cambrian|Cambrian|Most widespread outcropping Cambrian unit in the map area. Often caps hilltops. Trace fossils, Chancelloria spicules and acritarchs suggest correlation with Parachilna Formation. Fluvial gold trace was reported near Parara Mine.||||Unconformably overlies Doora Member. Locally occupies erosion channel in Moonta Porphyry Member. Overlain by Kulpara and Minlaton Formations.|Basal conglomerate; grading up into red-brown fluvial and quartzitic, medium-grained, cross-bedded, well-sorted and fossiliferous estuarine-shoreface sandstone; siltstone.|
20277|Winulta Formation|65686|6|Mentioned|p415|Early Cambrian|Early Cambrian|Clastics including mollusc fossils.||||||07-MAY-12
20277|Winulta Formation|65892|5|Briefly described|p9 Fig.4. |Early Cambrian|Early Cambrian|Yorke Peninsula.||||Is overlain by Kulpara Formation.||
20277|Winulta Formation|66761|5|Briefly described|p244, 246, 254|Cambrian|Cambrian|39 m interval in PIRSA stratigraphic hole Investigator 1. Better known from Yorke Peninsula.||||Underlies the ?Wangkonda Formation, overlies Donington Suite granite.|Grades up into 10 m of brecciated pale grey dolomite, some pyrite.|14-MAR-12
20277|Winulta Formation|67536|6|Mentioned|Map Legend||||||||Marine shelf to basinal carbonate, minor basal sandstone.|
20277|Winulta Formation|68735|6|Mentioned|p233 Fig.2, p235 Fig.3|Early Cambrian|Early Cambrian|Stansbury Basin.||||||
20277|Winulta Formation|68993|6|Mentioned|p544 Fig.1|Early Cambrian|Early Cambrian|Yorke Peninsula.||||||
20277|Winulta Formation|70382|5|Briefly described|p28|Early Cambrian|Early Cambrian|Geological province: Stansbury Basin.||||Overlain by Kulpara Formation.|Fluvial and coastal sandstone.|
20277|Winulta Formation|70833|5|Briefly described|p200|Cambrian|Cambrian|Of Western Stansbury Basin.||||Overlain unconformably by Kulpara Limestone.||
20277|Winulta Formation|73092|6|Mentioned|p2|Cambrian|Neoproterozoic|||||||
20277|Winulta Formation|73103|5|Briefly described|Map legend.|Cambrian|Cambrian|Appears with the map symbol Eo1 as a combined unit with Kulpara Formation.||||||
20277|Winulta Formation|73107|5|Briefly described|Map legend.|Early Cambrian|Early Cambrian|Stansbury Basin. Contains hyolithids, trace fossils, Plagiogmus arcuatus, Treptichnus pedum, Diplocraterion and acritarchs. Tommotian.|||||Arkosic sandstone to quartzite with minor siltstone and basal conglomerate. Uppermost part is dolomitic and silty.|
20277|Winulta Formation|73247|6|Mentioned|p205|Cambrian (Stage 2)|Cambrian (Stage 2)|"Yorke Peninsula. [Also written as ""Winulta Formation"" in the Kangaroo Island Investigator 1 Big Gully section; inferred to indicate tentative correlation]."||||Overlain by Kulpara Formation.||
20293|Wirrabara Formation|29780|6|Mentioned|p22|||||||||
20293|Wirrabara Formation|32725|6|Mentioned|p4|||Strat. table||||||
20293|Wirrabara Formation|37461|6|Mentioned|Table 5.I|||See also P337||||||
20293|Wirrabara Formation|41404|6|Mentioned|p76|||||||||
20293|Wirrabara Formation|44660|14|Not recorded|map legend|||Torrensian, lithology.||||||
20293|Wirrabara Formation|44690|4|Described|map legend|||Geol. Atlas Series. (I/54-5).||||||
20293|Wirrabara Formation|71237|14|Not recorded|p9, 19|||||||||
20293|Wirrabara Formation|71239|14|Not recorded|p5, p9, p19|||||||||
20297|Wirrapowie Limestone|22766|5|Briefly described|Fig.2 p561, p561|Early Cambrian|Early Cambrian|||||||
20297|Wirrapowie Limestone|23981|5|Briefly described|p8-9 Fig. 4, p10 Fig. 5|Early Cambrian|Early Cambrian|Overlies Parachilna Formation. Interfingers with Woodendinna Dolomite and Mernmerna Formation and passes laterally into lower Wilkawillina Limestone and Woodendinna Dolomite. Geological Province: Arrowie Basin.||||||04-FEB-08
20297|Wirrapowie Limestone|24465|5|Briefly described|p345 Fig.2|Early Cambrian|Early Cambrian|Of the Hawker Group.  Geological Province: Arrowie Basin.||||||19-JAN-05
20297|Wirrapowie Limestone|35255|6|Mentioned|Fig.8|||||||||
20297|Wirrapowie Limestone|36198|6|Mentioned|Fig.I.2|||||||||
20297|Wirrapowie Limestone|36244|6|Mentioned|p2|||Defined by Haslett 1975.||||||
20297|Wirrapowie Limestone|42011|6|Mentioned|p457|||||||||
20297|Wirrapowie Limestone|42225|6|Mentioned|Fig.4 P224|||||||||
20297|Wirrapowie Limestone|42233|6|Mentioned|p249|||||||||
20297|Wirrapowie Limestone|42440|6|Mentioned|Fig.2 P602|||||||||
20297|Wirrapowie Limestone|44133|5|Briefly described|p4 Fig. 7.2, 22|Early Cambrian|Early Cambrian|Geological Province: Arrowie Basin. Overlies: Woodendinna Dolomite. Overlies Parachilna Formation erosionally.||||||
20297|Wirrapowie Limestone|60418|5|Briefly described|p135|Early Cambrian|Early Cambrian|Of Hawker Group. Geological Province: Arrowie Basin of Adelaide Geosyncline.||||||
20297|Wirrapowie Limestone|60889|5|Briefly described|p247 Fig.4, p248-50|Early Cambrian|Early Cambrian|Thickness: 300 m. Contains the oldest archaeocyaths and trilobites in Australia. Arrowie Basin.|~530-529 Ma.|Hawker Group||Overlies Parachilna Formation and Woodendinna Dolomite. Basinal Wirrapowie Limestone transitions into shelfal lower Wilkawillina Limestone. Is overlain by lower Mernmerna Formation.|?silty limestone.|
20297|Wirrapowie Limestone|60959|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of the Hawker Group. Dark grey, laminated to mottled lime mudstone and fine-grained limestone with oolite, stromatolite and thrombite.||||||
20297|Wirrapowie Limestone|60990|6|Mentioned|p83 Fig.2|Atdbanian|Atdbanian|Flinders Ranges.||Hawker Group.||||
20297|Wirrapowie Limestone|62592|5|Briefly described|p50 Table 5.1.|Early Cambrian|Early Cambrian|Adelaide Geosyncline.||Unit in Hawker Group.||Overlies Woodendinna Dolomite. Is overlain by Wilkawillina Limestone.|Nodular and stromatolitic limestone.|
20297|Wirrapowie Limestone|62783|6|Mentioned|p1, p2 Fig.1, p3||Early Cambrian|Contains shells of paterinate brachiopod Askepasma sp. penetrated by phosphatic canals that most likely contained organic setae.||||||
20297|Wirrapowie Limestone|63447|6|Mentioned|p963 Fig.2 |Early Cambrian|Early Cambrian|||||Shown as partial lateral equivalent of Woodendinna Dolomite, lower Wilkawillina Limestone.||
20297|Wirrapowie Limestone|63569|6|Mentioned|p117 Fig.1|Early Cambrian|Early Cambrian|Arrowie Basin.||||||
20297|Wirrapowie Limestone|65686|6|Mentioned|p413, 415 Fig 4|Early Cambrian|Early Cambrian|Arrowie Basin. Includes brachiopods.||||||07-MAY-12
20297|Wirrapowie Limestone|65892|5|Briefly described|p8, p9 Fig.4, p27-28. |Early Cambrian|Early Cambrian|Arrowie Basin. Contains the oldest archaeocyaths and trilobites in Australia. Depositional structures indicate a peritidal environment.||Unit in Hawker Group.||Overlies Parachilna Formation.||
20297|Wirrapowie Limestone|65925|5|Briefly described|p14 Fig.2.2, Appendix 2.|Early Cambrian|Early Cambrian||||||Limestone and calcareous siltstone, green and grey, stromatolitic, intraformational conglomerate; minor cross-bedded ooid grainstone.|
20297|Wirrapowie Limestone|67870|6|Mentioned|p21|Cambrian|Cambrian|Provides a surface constraint on seismic line 09TE-03.||||||
20297|Wirrapowie Limestone|68030|6|Mentioned|p239|||Flinders Ranges.||||Unconformably overlain by the Mernmerna Formation.||
20297|Wirrapowie Limestone|68735|5|Briefly described|p233-235|Early Cambrian|Early Cambrian|Arrowie Basin.||Of the Hawker Group.||Underlain by the Parachilna Formation. Overlain and intertongued by the lower Wilkawilline Limestone.|Comprises laminated micritic limestone with tongues of ooid grainstones, plus thrombolites, stromatolites and archaeocyath-Renalcis bioherms.|10-APR-17
20297|Wirrapowie Limestone|68993|6|Mentioned|p544 Fig.1|Early Cambrian|Early Cambrian|Arrowie Basin.||Of the Hawker Group.||||
20297|Wirrapowie Limestone|69570|5|Briefly described|p421 fig 1-p426, p428, p430, p432, p435|Cambrian|Cambrian|Arrowie Syncline, Flinder Ranges. Appears as Wirrapowie Formation on p422. Approximately 139m thick in the Moro section. Fossil assemblage and sample localities are described.||||Interfingered with the Winnitinniy Creek Member and partially overlies it.|Fine-grained ribbon limestones, intepreted to be deposited in a lagoonal environment.|
20297|Wirrapowie Limestone|70833|5|Briefly described|p176,178-182,184,189-194,196-198|Series 2|Terreneuvian|Of Arrowie Basin. Key sections: MORO and MOG (S of Moro Gorge, Arrowie Syncline); WAR (Warragee Bore, central Flinders Ranges); CR1 (Chace Range, S Flinders Ranges). Coeval with Wilkawillina Limestone. Depositional environment: deeper outer shelf facies.  Includes K. rostana zone in the 430m of the section in the WAR and CR1 section, M. etheridgei zone. Time-equivalent to uppermost Kulpara Limestone and lower half of Heatherdale Shale. See also p200-201,205. Correlable to Wilkawillina and Ajax limestones.||Unit of Hawker Group.||Overlain unconformably by Mernmerna Formation. Underlain by Woodendinna Dolostone.||
20297|Wirrapowie Limestone|70835|6|Mentioned|p334-336, 345, 352|Cambrian|Cambrian|Chace Range, southern Flinders Ranges. Contains helcionellid molluscs; systematic paleontology descriptions, photographs. Up to 904m thick.||||Overlies Woodendinna Dolostone. Is overlain by Mernmerna Formation.|Predominantly nodular limestone; upper part comprises poorly-outcropping ferruginous shale.|
20297|Wirrapowie Limestone|71102|4|Described|p242-243,247-249,251,265-267,271, 274|Series 2|Terreneuvian|Of Arrowie Basin. Definition at type section by Hallett 1975: "overlain by Parara-type limesstones, and more specifically, the uppermost Wirrapowie Limestone is "selected at the top of the upper most algal stromatolitic bed", and also "gradational into Parara Limestone". This definition makes identification of the boundary between Wirrapowie Limestone and Mernmerna Formation ambiguous away from type section. Intersected section: ER9 (Elder Range, Southern Flinders Ranges), BHG (Bullock Head Gap, SW Arrowie Syncline), RC (Rainwater Creek, S Arrowie Syncline). Fossil assemblage described.||||Overlain by, and interfingers with Mernmerna Formation.|Micritic, ribbon to nodular limestone with interbedded muds and microbial laminations. Occasional oolites/brecciated intervals.|05-SEP-19
20300|Wirrealpa Limestone|22631|6|Mentioned|p178|Cambrian|Cambrian|||||||
20300|Wirrealpa Limestone|22766|5|Briefly described|Fig.2 p561, p562|Early Cambrian|Early Cambrian|||||||
20300|Wirrealpa Limestone|22772|5|Briefly described|Table 13.1|Middle Cambrian|Early Cambrian|||||||
20300|Wirrealpa Limestone|22857|5|Briefly described|Tb 13.1 (insert p70-71), p90 Fig. 14.7B|Middle Cambrian|Early Cambrian|Of Lake Frome Group. Age: ~509Ma. Geological Province: Arrowie Basin.||||||
20300|Wirrealpa Limestone|22858|6|Mentioned|p92,Fig14.7bp90-1|||||||||
20300|Wirrealpa Limestone|23155|6|Mentioned|p9|||Equivalent to the Kalladeina Formation (eastern Warburton Basin).||||||
20300|Wirrealpa Limestone|23250|5|Briefly described|p1124 Fig.2||Early Cambrian|Age: Stage 4 of Early Cambrian. Correlate of Yarrawurta Shale.||||||
20300|Wirrealpa Limestone|23818|5|Briefly described|p51 Fig.16|Cambrian|Cambrian|||||||18-APR-05
20300|Wirrealpa Limestone|23981|6|Mentioned|p8-9 Fig. 4|Toyonian|Toyonian|Overlies Billy Creek Formation; underlies Lake Frome Group. Geological Province: Arrowie Basin.||||||04-FEB-08
20300|Wirrealpa Limestone|24072|5|Briefly described|p369 Fig.1|Cambrian|Cambrian|Geological Province: Great Artesian Basin.||||||
20300|Wirrealpa Limestone|24138|5|Briefly described|p32|Cambrian|Cambrian|Marine. Contains abundant trilobites, brachiopods, sponge spicules and algae. Geological Province: Adelaide Geosyncline.||||||
20300|Wirrealpa Limestone|24176|5|Briefly described| p17|Middle Cambrian|Middle Cambrian|Treated as undifferentiated from Aroona Creek Limestone (COPLEY) in these Notes (p23 Tb. 1) and referred to as Wirrealpa Limestone-Aroona Creek Limestone (undifferentiated).  Overlain by Moodlatana Fm.(Lake Frome Gp.)||||||
20300|Wirrealpa Limestone|24465|5|Briefly described|p345 Fig.2|Middle Cambrian|Early Cambrian|Geological Province: Arrowie Basin.||||||19-JAN-05
20300|Wirrealpa Limestone|29929|6|Mentioned|Fig.4|||||||||
20300|Wirrealpa Limestone|30051|6|Mentioned|Fig.12|||See also p28. Middle Cambrian age.||||||19-DEC-06
20300|Wirrealpa Limestone|30176|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
20300|Wirrealpa Limestone|30511|6|Mentioned|p47|||||||||
20300|Wirrealpa Limestone|30544|6|Mentioned|p49|||||||||
20300|Wirrealpa Limestone|30801|6|Mentioned|p5|||Table p5-6.||||||19-DEC-06
20300|Wirrealpa Limestone|30802|5|Briefly described|p11|||Lower Middle Cambrian.||||||
20300|Wirrealpa Limestone|30807|6|Mentioned|p102|||Suggested map symbol||||||
20300|Wirrealpa Limestone|31539|6|Mentioned|Fig. 28|||||||||
20300|Wirrealpa Limestone|31706|6|Mentioned|p633|||Cambrian correlation chart||||||
20300|Wirrealpa Limestone|31797|6|Mentioned|Fig. 2|||M.Camb. of Lake Frome Group.||||||19-DEC-06
20300|Wirrealpa Limestone|32669|6|Mentioned|p523|||M.Camb.||||||
20300|Wirrealpa Limestone|33332|6|Mentioned|p15|||M.Cambrian.||||||
20300|Wirrealpa Limestone|33474|6|Mentioned|Fig.3|||||||||
20300|Wirrealpa Limestone|33932|6|Mentioned|p14|||||||||
20300|Wirrealpa Limestone|33934|6|Mentioned|Fig.2|||M - U Camb.||||||
20300|Wirrealpa Limestone|33972|4|Described|p14|||Mention p13.||||||19-DEC-06
20300|Wirrealpa Limestone|33973|6|Mentioned|Fig.2|||||||||
20300|Wirrealpa Limestone|34269|6|Mentioned|Table 1|||||||||
20300|Wirrealpa Limestone|34535|6|Mentioned|Fig.16|||Cambrian||||||
20300|Wirrealpa Limestone|34612|6|Mentioned|Fig.33|||Cambrian||||||
20300|Wirrealpa Limestone|34812|6|Mentioned|Table 9|||||||||
20300|Wirrealpa Limestone|35255|6|Mentioned|Fig.8|||||||||
20300|Wirrealpa Limestone|35798|6|Mentioned|Fig.4|||Correlation of lower units in Desert Syncline drill holes.||||||
20300|Wirrealpa Limestone|35835|6|Mentioned|p207|||||||||
20300|Wirrealpa Limestone|35954|6|Mentioned|p1230|||See also Fig.2.||||||
20300|Wirrealpa Limestone|36137|6|Mentioned|Fig.2|||||||||
20300|Wirrealpa Limestone|36198|6|Mentioned|p249|||See also Fig.I.2||||||
20300|Wirrealpa Limestone|36495|6|Mentioned|p127|||||||||
20300|Wirrealpa Limestone|36525|6|Mentioned|Fig.4|||See also Fig.5.||||||
20300|Wirrealpa Limestone|37802|6|Mentioned|Fig.2|||||||||
20300|Wirrealpa Limestone|38004|6|Mentioned|Table 1|||||||||
20300|Wirrealpa Limestone|38068|6|Mentioned|p69|||See also Fig.4.||||||
20300|Wirrealpa Limestone|39344|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
20300|Wirrealpa Limestone|39352|6|Mentioned|Map legend|Late Cambrian|Middle Cambrian|Middle to Late Cambrian||||||
20300|Wirrealpa Limestone|40455|6|Mentioned|Fig.2|||||||||
20300|Wirrealpa Limestone|40852|6|Mentioned|p33|||||||||
20300|Wirrealpa Limestone|40856|6|Mentioned|Fig.23.6|||||||||
20300|Wirrealpa Limestone|40914|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
20300|Wirrealpa Limestone|41401|6|Mentioned|p32|||||||||
20300|Wirrealpa Limestone|41496|5|Briefly described|Fig.1|||||||||
20300|Wirrealpa Limestone|41526|6|Mentioned|p60|||||||||
20300|Wirrealpa Limestone|42090|6|Mentioned|p26|||||||||
20300|Wirrealpa Limestone|42141|6|Mentioned|Table 2 P571|||||||||
20300|Wirrealpa Limestone|42192|6|Mentioned|p14|||||||||
20300|Wirrealpa Limestone|42225|6|Mentioned|p223|||||||||
20300|Wirrealpa Limestone|42266|6|Mentioned|Fig.2 P292|||||||||
20300|Wirrealpa Limestone|42269|6|Mentioned|p337|||||||||
20300|Wirrealpa Limestone|42272|6|Mentioned|p414|||||||||
20300|Wirrealpa Limestone|42357|5|Briefly described|p10|||||||||
20300|Wirrealpa Limestone|42440|4|Described|p601, p611|||||||||
20300|Wirrealpa Limestone|42573|5|Briefly described|Fig.1 P190|||||||||
20300|Wirrealpa Limestone|43011|6|Mentioned|Table 2,p12|||||||||
20300|Wirrealpa Limestone|43053|5|Briefly described|Map Legend|Cambrian|Cambrian|Shallow marine to terrestrial redbeds, peritidal to marine limestone.||||||25-MAY-05
20300|Wirrealpa Limestone|43258|5|Briefly described|Map Legend||Cambrian|||||||
20300|Wirrealpa Limestone|43298|6|Mentioned|Map Legend||Cambrian|||||||
20300|Wirrealpa Limestone|43781|6|Mentioned|p4||Middle Cambrian|||||||
20300|Wirrealpa Limestone|43845|6|Mentioned|Fig 4 p44|||||||||12-JUL-16
20300|Wirrealpa Limestone|44040|14|Not recorded|p38|||||||||
20300|Wirrealpa Limestone|44093|5|Briefly described|p138 App. 1|Middle Cambrian|Early Cambrian|Geological Province: Adelaide Fold Belt.||||||
20300|Wirrealpa Limestone|44133|5|Briefly described|p4 Fig. 7.2, 5, 17, 27, 29 Fig. 7.13|Early Cambrian|Early Cambrian|Geological Province: Arrowie Basin. Maximum Thickness: 135m.||||||
20300|Wirrealpa Limestone|45055|6|Mentioned|p6|||Location||||||
20300|Wirrealpa Limestone|45102|6|Mentioned|p48|||||||||
20300|Wirrealpa Limestone|45155|6|Mentioned|Fig.8|||||||||
20300|Wirrealpa Limestone|60418|6|Mentioned|p134 Fig.1|||||||||
20300|Wirrealpa Limestone|60419|5|Briefly described|p18|Middle Cambrian|Middle Cambrian|Geological Province: Adelaide Rift.  Contains fauna of Ordian age.||||||
20300|Wirrealpa Limestone|60889|5|Briefly described|p245 Fig.2, p247-9, p251-4|Early Cambrian|Early Cambrian|Shallow marine carbonates. Thickness: 120 m. Arrowie Basin. Primary dilling target (Moorowie-1).|>512 Ma.|||Overlies Billy Creek Formation. Is overlain (unconformably?) by Moodlatana Formation (basal Lake Frome Group).|Carbonates. Widespread; a potential reservoir-seal couplet where oolitic reservoir is overlain by micrite seal.|
20300|Wirrealpa Limestone|60953|5|Briefly described|Map Legend|Cambrian|Cambrian|Geological Province: Arrowie Basin.||||||
20300|Wirrealpa Limestone|60959|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of the Lake Frome Group. Lime mudstone, nodular limestone in a calcareous silty matrix.||||||
20300|Wirrealpa Limestone|60990|5|Briefly described|p83 Fig.2, p85 |Toyonian|Toyonian|Flinders Ranges. Faunal links with Antarctica.||||||
20300|Wirrealpa Limestone|61108|5|Briefly described|map legend|Cambrian|Cambrian|Shallow marine to terrestrial redbeds; peritidal to marine limestone. Geological Province: Arrowie Basin.||||||03-JUN-05
20300|Wirrealpa Limestone|62592|5|Briefly described|p50 Table 5.1, p59.|Early Cambrian|Early Cambrian|Adelaide Geosyncline.||Unit in Moralana Supergroup.||Overlies Billy Creek Formation. Is overlain by Lake Frome Group.|Fossiliferous limestone.|
20300|Wirrealpa Limestone|62784|5|Briefly described|p8 Fig.1|Cambrian|Cambrian|Arrowie Basin. Overlies Billy Creek Formation and is overlain by Moodlatana Formation of the Lake Frome Group.||||||
20300|Wirrealpa Limestone|62787|5|Briefly described|p82, p82 Fig. 3|Early Cambrian|Neoproterozoic|Geological Province: Arrowie Basin (SA).||||||07-FEB-11
20300|Wirrealpa Limestone|63447|6|Mentioned|p963 Fig.2 |Early Cambrian|Early Cambrian|Arrowie Basin||||Overlies Billy Creek Formation. Aroona Creek Limestone shown as lateral equivalent.||
20300|Wirrealpa Limestone|63489|5|Briefly described|Map legend|Middle Cambrian|Early Cambrian|Marine limestone.||||||10-SEP-07
20300|Wirrealpa Limestone|63569|4|Described|pp116-120, pp122-123, p125 Fig. 6|Early Cambrian|Early Cambrian|Arrowie Basin, Adelaide Geosyncline. 105-140 m thick transgressive-regressive carbonate sequence with lagoonal and ooid bank megafacies. Abundantly fossiliferous.||||Conformably overlies Billy Creek Formation. Is conformably overlain by Moodlatana Formation.|Lime mudstone; nodular limestone with calcareous silty matrix; skeletal, peloidal and oolitic beds; stromatolite and thrombolite bioherms; micrite; siltstone.|
20300|Wirrealpa Limestone|64829|5|Briefly described|p1084-5 Figs.1,  2|Early Cambrian|Early Cambrian|Unit discussed in the context of soilscapes and palaeosols. Basal section contains the trilobite, Redlichia guizhouensis.||||||07-FEB-11
20300|Wirrealpa Limestone|65313|5|Briefly described|p577, p576 Fig. 5,  p578 Fig. 6|Middle Cambrian|Middle Cambrian|Trilobites in this unit at Ten Mile Creek section eastern Arrowie Basin, correlated with 511.5 Ma R. gulzhouensis trilobite zone. Shown as Arcadian age in Fig. 6||||Underlies Lake Frome Group.||26-MAR-12
20300|Wirrealpa Limestone|65375|5|Briefly described|p33.|Early Cambrian|Early Cambrian|||||Overlies Billy Creek Formation. Is overlain by Moodlatana Formation.||
20300|Wirrealpa Limestone|65625|5|Briefly described|p103 Fig.2|Middle Cambrian|Middle Cambrian|Lake Frome area.||||Overlies Billy Creek Formation. Underlies Lake Frome Group.||18-FEB-11
20300|Wirrealpa Limestone|65686|5|Briefly described|p411, 413, 415, p409 Fig 2|Early Cambrian|Early Cambrian|Arrowie Basin. Contains the youngest archaeocyath in Australia. 120m thick.||||||07-MAY-12
20300|Wirrealpa Limestone|65892|4|Described|p9 Fig.4, p10,p12, p38-39, p41, p45-46  |Early Cambrian|Early Cambrian|Arrowie Basin. 120m thick. Shallow marine carbonates. Contains Redlichia guizhouensis and the youngest archaeocyath fauna in Australia.|c.520 Ma.|||Overlies Billy Creek Formation. Is overlain by Moodlatana Formation. Equivalent to Aroona Creek Limestone.|Grey limestone; fossiliferous.|
20300|Wirrealpa Limestone|65925|5|Briefly described|p14 Fig.2.2, Appendix 2.|Early Cambrian|Early Cambrian||||||Medium grey micritic limestone; basal dolomite.|
20300|Wirrealpa Limestone|66518|6|Mentioned|p19 Fig.4.|Cambrian|Cambrian|Arrowie Basin.||||Overlies Billy Creek Formation. Is overlain by Moodlatana Formation.||
20300|Wirrealpa Limestone|67536|5|Briefly described|Map Legend|Stage 2|Stage 2||ca. 523 +/- 2 Ma||||Shallow marine to terrestrial redbeds, peritidal to marine limestone|
20300|Wirrealpa Limestone|67870|6|Mentioned|p5, p9, p23-25|Cambrian|Cambrian|Arrowie Basin. Appears as Wirrealpa Formation on p9; and as Wirrealpa-Lake Frome Group on p25.||||||
20300|Wirrealpa Limestone|68030|5|Briefly described|p239|Cambrian|Cambrian|Flinders Ranges.||||Overlain by Lake Frome Group. Underlain unconformably by Billy Creek Formation.||
20300|Wirrealpa Limestone|68735|4|Described|p231, pp233-239|Early Cambrian|Early Cambrian|Arrowie Basin. Described by Youngs (1977). ~ 120 m thick. Contains abundant trilobites, brachiopods, and small shelly fossils. Also described are cyanobacterial-archaeocyathan-radio-cyathan bioherms (Kruse 1991): youngest archaeocyaths in Australia.||||Overlies Billy Creek Formation. Overlain by the Lake Frome Group. Is equivalent to Aroona Creek Limestone.|Comprises shallow marine carbonates at the top and bottom with slightly deeper water shales in the middle.|10-APR-17
20300|Wirrealpa Limestone|68993|6|Mentioned|p544 Fig.1|Early Cambrian|Early Cambrian|Arrowie Basin.||||||
20300|Wirrealpa Limestone|69570|6|Mentioned|p421 fig 1|Cambrian|Cambrian|Arrowie Syncline, Flinder Ranges.||||||
20300|Wirrealpa Limestone|69982|5|Briefly described|p19|||Arrowie Basin. Older than Templetonian-Floran, and younger than Botomian: age from surrounding units.||||May correlate with Diamond Bog Dolomite (Warburton Basin).||
20300|Wirrealpa Limestone|70752|6|Mentioned|p133|||Brachiopod fossil briefly discussed.||||||
20300|Wirrealpa Limestone|70833|6|Mentioned|p200|||Of Arrowie Basin.||||Underlain by Billy Creek Formation.||
20300|Wirrealpa Limestone|70835|6|Mentioned|p335|Cambrian|Cambrian|Arrowie Basin, Flinders Ranges.||||||
20300|Wirrealpa Limestone|72449|5|Briefly described|p1, p2 Map Legend|Cambrian|Cambrian|Shown as part of diapir formation diagram, p1.||||Overlies Billy Creek Formation and underlies Moodlatana Formation|Wavy bedded to nodular limestone in a silty matrix. Algal mats and stromatolites are common; fossil trilobites and brachiopods occuring.|
20300|Wirrealpa Limestone|73251|6|Mentioned|p36|Cambrian|Cambrian|Arrowie Basin, Moorowie and Yalkalpo Sub-basins. Thermally late to post-mature.||||Underlain by Billy Creek Formation. Overlain by Moodlatana Formation (Lake Frome Group).||
20300|Wirrealpa Limestone|73255|6|Mentioned|p534 Fig.2|early Cambrian|early Cambrian|Contains Redlichia guizhouensis trilobite fossils.||||Overlies the Billy Creek Formation, underlies the Moodlatana Formation.|Carbonate rocks.|
20307|Wirrildar beds|23282|6|Mentioned|p72|||May correlate with Observatory Hill Formation. of central Officer Basin.||||||
20307|Wirrildar beds|23288|6|Mentioned|Fig.5|||||||||
20307|Wirrildar beds|31969|3|Fully described|p8|||See also P9-10||||||
20307|Wirrildar beds|36701|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
20307|Wirrildar beds|43052|5|Briefly described|Table 2.1|||||||||
20307|Wirrildar beds|43053|5|Briefly described|Map Legend|Cambrian|Cambrian|Feldspathic sandstone, siltstone and dolomite.||||||25-MAY-05
20307|Wirrildar beds|43258|5|Briefly described|Map Legend||Cambrian|||||||
20307|Wirrildar beds|43298|5|Briefly described|Map Legend||Cambrian|||||||
20307|Wirrildar beds|44133|5|Briefly described|p39, 42, 4 Fig. 7.2|Middle Paleozoic|Early Paleozoic|Geological Province: Eastern Officer Basin. Overlies: Punkerri Sandstone (un). Underlies: Kulyong Volcanics (un).||||||07-NOV-08
20307|Wirrildar beds|60953|5|Briefly described|Map Legend|Cambrian|Cambrian|Feldspathic sandstone, siltstone and dolomite.||||||
20307|Wirrildar beds|61108|5|Briefly described|map legend|Cambrian|Cambrian|Feldspathic sandstone, siltstone and dolomite.||||||
20307|Wirrildar beds|61732|6|Mentioned|p79|Cambrian|Cambrian|Geological Province: Birksgate Sub-basin.||||||07-FEB-11
20307|Wirrildar beds|65416|5|Briefly described|p144.|||Correlated with McFadden Formation. Written as Wirrildar Beds on p144.||||Overlies Punkerri Sandstone. Is unconformably overlain by Kulyong Volcanics and Table Hill Volcanics.||
20307|Wirrildar beds|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.|
20307|Wirrildar beds|67921|5|Briefly described|Map legend|Cambrian|Cambrian|Grouped with Arcoeillina Sandstone and Observatory Hill Formation. Group description: Fluvial, lacustrine, aeolian and sabkha deposits including micaceous and feldspathic sandstone and mudstone, cherty (Magadi-type) siltstone and carbonate interbeds.||||||
20307|Wirrildar beds|69091|5|Briefly described|p35|||Predates Late Cambrian Table Hill Volcanics, suggests gentle folding is due to Delamerian Orogeny.|||||Thick, gently folded sandstone succession.|
20307|Wirrildar beds|70793|4|Described|500k_interpgeop14_lut.csv|Series 2|Cambrian|Of Officer Basin (Phase 1), Centralian Superbasin. Events: Officer Basin Cenozoic diapirism (66-0.01 Ma); Delamarian Orogeny (520-505 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma). See 500k_interpgeop14_lut.csv, 2_5m_interpgeop15_lut.csv.|541-509 Ma (inferred)||||Fine grained, micaceous sandstone and dolomite, with basal arkosic sandstone; fines and becomes more calcareous upwards|
20307|Wirrildar beds|70826|6|Mentioned|p7 tbl 3|Cambrian|Cambrian|Officer Basin.||||||
20307|Wirrildar beds|71146|5|Briefly described|p6, p21|Cambrian|Neoproterozoic|Officer Basin.||||Unconformably overlain by the Table Hill Volcanics.|Sandstone.|
20307|Wirrildar beds|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||arkose|
20307|Wirrildar beds|71268|4|Described|GEOL_LUT_CSV files|Series 2|Cambrian|Of Officer Basin (Phase 1), Centralian Superbasin. Events: Officer Basin Cenozoic diapirism (66-0.01 Ma); Delamerian Orogeny (520-505 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma). See 250k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv.|541-511 Ma (inferred)|Unit of Marla Group.|||Fine-grained micaceous sandstone and dolomite, with basal arkosic sandstone; fines and becomes more calcareous upwards|
20307|Wirrildar beds|72034|5|Briefly described|500k_interpgeop16_lut|Series 2|Cambrian|Officer Basin (Phase 1).|||||Fine grained, micaceous sandstone and dolomite, with basal arkosic sandstone; fines and becomes more calcareous upwards.|
20307|Wirrildar beds|73100|5|Briefly described|Map legend|Cambrian|Cambrian|Subsurface. Mapped as one unit with Arcoeillina Sandstone and Observatory Hill Formation.||||||
20307|Wirrildar beds|73111|5|Briefly described|Map legend.|Cambrian|Cambrian|Mapped as one unit with Arcoeillina Sandstone and Observatory Hill Formation. Subcrop and minor outcrop.|||||Fluvial, lacustrine, aeolian and sabkha deposits including micaceous and feldspathic sandstone and mudstone, cherty (Magadi-type) siltstone and carbonate interbeds.|
20313|Witchelina Quartzite|9862|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Of the Burra Group. Well bedded feldspathic quartzite, shwing cross-bedding and minor heavy mineral lamination.||||||
20313|Witchelina Quartzite|22772|5|Briefly described|Table13.1|Cryogenian|Cryogenian|||||||
20313|Witchelina Quartzite|22857|5|Briefly described|Tb. 13.1 (insert p70-71)|Torrensian|Torrensian|Of the Emeroo Subgroup (Burra Group).||||||
20313|Witchelina Quartzite|22869|6|Mentioned|P46|||Correlated to the Carey Gully Sandstone Member||||||
20313|Witchelina Quartzite|22889|6|Mentioned|p31|Adelaidean|Adelaidean|Parent - Emeroo Subgroup.||||||
20313|Witchelina Quartzite|23818|5|Briefly described|p55|||Underlying unit: Equivalent of Wortupa Quartzite and Rhynie Sandstone.||||||
20313|Witchelina Quartzite|24175|3|Fully described|p11|Neoproterozoic|Neoproterozoic|Of Emeroo Subgroup (Burra Group). Overlain by Skillogalee Dolomite; underlain transitionally by Willawalpa Formation. Max. thickness: 940m.||||||13-FEB-08
20313|Witchelina Quartzite|24321|5|Briefly described|Map legend|Adelaidean|Adelaidean|Parent: Emeroo Subgroup||||||
20313|Witchelina Quartzite|30177|6|Mentioned|p47|||||||||
20313|Witchelina Quartzite|30807|6|Mentioned|p103|||Suggested map symbol||||||
20313|Witchelina Quartzite|34535|6|Mentioned|p59|||Equiv. Rhynie Sst.||||||
20313|Witchelina Quartzite|36733|6|Mentioned|p12|||||||||
20313|Witchelina Quartzite|37854|2|Defined|p14|Adelaidean|Adelaidean|See also P13. Early Torrensian||||||
20313|Witchelina Quartzite|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Torrensian||||||
20313|Witchelina Quartzite|40294|6|Mentioned|p8|||||||||
20313|Witchelina Quartzite|41403|6|Mentioned|p43|||||||||
20313|Witchelina Quartzite|41404|3|Fully described|p88|||||||||
20313|Witchelina Quartzite|42222|6|Mentioned|Table 1 P5|||||||||
20313|Witchelina Quartzite|42238|6|Mentioned|p73|||||||||
20313|Witchelina Quartzite|43052|5|Briefly described|p177|||of Emeroo Subgroup||||||
20313|Witchelina Quartzite|44689|14|Not recorded|map legend|||Andamooka. (H53-12).||||||
20313|Witchelina Quartzite|60718|5|Briefly described|p49, 52|Adelaidean|Adelaidean|Max. thickness: 1200m. Geological Province: Adelaide Geosyncline. See also p51 Fig. 3.|||Of Emeroo Subgroup (Burra Group).|Passes up into Skillogalee Dolomite.||15-APR-11
20313|Witchelina Quartzite|60955|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Of the Burra Group. Massive and flaggy, well beddded quartzites.||||||
20313|Witchelina Quartzite|66884|5|Briefly described|p36, p39 Fig.2, p41 Fig.3|||Thickness: up to 2400 m.||Emeroo Subgroup||Overlies Willawalpa Formation.|Subarkose to quartz arenite (grey to tan, fine-coarse grained, well sorted, medium bedded, flaggy, ripple cross-laminations, clay intraclasts and desiccation cracks) interbedded with subordinate ripple cross-laminated siltstone and shale.|
20313|Witchelina Quartzite|69019|4|Described|p39-40, p134, p135 Fig.30.|Neoproterozoic|Neoproterozoic|Described by Sprigg (1949) and Thomson et al. (1964); type section proposed by Forbes et al. (1981) in Old Norwest Gorge, where it is 1,200 m thick. Resistant unit, forming prominent outcrops in eastern Willouran Ranges.||Unit in Emeroo Subgroup.||Transitionally overlies Willawalpa Formation. Is overlain conformably by Skillogalee Dolomite.|Flaggy to medium bedded, pale grey to pale brown, feldspathic quartzite and arkose, and lesser grey shale.|
20313|Witchelina Quartzite|71237|14|Not recorded|p10|||||||||
20313|Witchelina Quartzite|71239|14|Not recorded|p3, 4, 10|||Base of the Burra Group in the Willouran Ranges.||||||
20313|Witchelina Quartzite|71240|14|Not recorded|p6, p10|||||||Correlated with Rhynie Sandstone.||
20313|Witchelina Quartzite|72456|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Marree 1:250k map sheet.|||||Quartzite, sandstone and shale.|
20340|Wockerawirra Dolomite|30801|6|Mentioned|p5|||Table P5-6||||||
20340|Wockerawirra Dolomite|30802|4|Described|Table 1|||Sturtian age.||||||
20340|Wockerawirra Dolomite|32510|6|Mentioned|Fig.1|||||||||
20340|Wockerawirra Dolomite|32724|6|Mentioned|Fig.1|||Correlation. Sturtian||||||
20340|Wockerawirra Dolomite|34267|6|Mentioned|Fig.|||The Oraparinna & Enorama diapiric structures.||||||
20340|Wockerawirra Dolomite|34269|6|Mentioned|Table 1|||||||||
20340|Wockerawirra Dolomite|34291|6|Mentioned|p12|||||||||
20340|Wockerawirra Dolomite|35075|6|Mentioned|p77|||||||||
20340|Wockerawirra Dolomite|35255|6|Mentioned|Fig.18|||||||||
20340|Wockerawirra Dolomite|35582|6|Mentioned|p51|||||||||
20340|Wockerawirra Dolomite|42109|6|Mentioned|p23|||||||||
20340|Wockerawirra Dolomite|62592|5|Briefly described|p50 Table 5.1.|Sturtian|Sturtian|Adelaide Geosyncline.||Unit in Nepouie Subgroup.||Overlies Tapley Hill Formation.|Dolomite.|
20340|Wockerawirra Dolomite|62903|6|Mentioned|p730 Fig.1|||Adelaide Rift Complex. Presented in figure as Wockerawirra, and associated with the Tapley Hill Formation in stratigraphic column.||||relationship with Tapley Hill Formation not specified.||
20340|Wockerawirra Dolomite|64797|6|Mentioned|p153 Fig.2|Cryogenian|Cryogenian|Adelaide Rift Complex. Lithology/rank not shown on diagram.||||||
20340|Wockerawirra Dolomite|67979|4|Described|p538-540, p529-530, p537 Fig.8, p542-545|Marinoan|Marinoan|This article describes a major disconformity between Wockerawirra Dolomite and underlying Tapley Hill Formation, and suggests that Wockerawirra Dolomite should be considered as basal member of Sunderland Formation (Upalinna Subgroup). Type locality: Oraparinna section in Central Flinders Ranges (Fig.8). Both sections described are deep marine laminated limestone horizons (not dolomite). The lower Yankaninna Formation is considered a time-equivalent succession. See also Fig. 1, Wockerawirra Dolomite Member in Fig.2 (p531).||||erosionally overlies (with some angularity) transitional shale unit of Tapley Hill Formation; gradationally conformable beneath Sunderland Formation; correlated with lower Yankaninna Formation.|deep water laminated limestones (not dolomite), relatively pure carbonates|
20340|Wockerawirra Dolomite|71237|14|Not recorded|p10, 19|||||||||
20340|Wockerawirra Dolomite|72429|5|Briefly described|p958|Proterozoic|Proterozoic|Occurs as a prominent yellow-weathered resistant capping to high ridges above the flat-lying Tapley Hill Formation at Mt Chambers.||Umberatana Group||Disconformably overlies the Tapley Hill Formation.|Yellow-weathered dolomite.|
20340|Wockerawirra Dolomite|72601|6|Mentioned|p5|||[ambiguous use; see Wockerawirra Member].||Umberatana Group||||
20402|Wombat Sandstone Member|22485|5|Briefly described|p51 , Fig 2|Late Cretaceous|Late Cretaceous|||||||
20402|Wombat Sandstone Member|42545|3|Fully described|p11|Coniacian|Cenomanian|Of Wigunda Formation. Probably NOT variation on Wombat Group or Wombat Creek Group, Vic.||||||31-JAN-08
20402|Wombat Sandstone Member|43814|6|Mentioned|Fig.3,p115|||||||||
20402|Wombat Sandstone Member|44133|5|Briefly described|p141|Coniacian|Turonian|Conformably overlies: Platypus Formation. Of the Wigunda Formation. Maximum Thickness: 103m.||||||
20402|Wombat Sandstone Member|63124|5|Briefly described|p79|||Of Wigunda Formation. Geological Province: Duntroon Basin. May be correlated with Waarre Sandstone (Sherbrook Group).||||||
20402|Wombat Sandstone Member|69297|5|Briefly described|p14 fig 2.4, p25 fig 2.9, p60|Coniacian|Turonian|Ceduna and Duntroon Sub-basins.||Wigunda Formation||Overlies the Platypus Formation.|Sandstone and siltstone.|
20402|Wombat Sandstone Member|70067|5|Briefly described|Ceduna: Fig.2. Regional: Fig.2|Turonian|Cenomanian|Duntroon Sub-basin, Bight Basin.||Wigunda Formation.||||
20468|Woocalla Dolomite Member|22510|5|Briefly described|table1p37|||Of the Tapley Hill Formation.  Age: Sturtian. Stuart Shelf||||||13-OCT-04
20468|Woocalla Dolomite Member|22829|6|Mentioned|Fig2 P17|||||||||
20468|Woocalla Dolomite Member|23913|4|Described|p110 Fig. 2|Adelaidean|Adelaidean|Geological Province: Stuart Shelf.  Of the Umberatana Group.  Intrudes the Tapley Hill Formation.||||||
20468|Woocalla Dolomite Member|24476|4|Described|p547 Fig. 4|Adelaidean|Adelaidean|Of the Tapley Hill Formation. Geological Province: Stuart Shelf||||||
20468|Woocalla Dolomite Member|31541|6|Mentioned|p545|||||||||
20468|Woocalla Dolomite Member|35003|6|Mentioned|p122|||||||||
20468|Woocalla Dolomite Member|35255|5|Briefly described|p9|||See also Fig.6.||||||
20468|Woocalla Dolomite Member|35678|6|Mentioned|p64|||Summary geological logs.||||||
20468|Woocalla Dolomite Member|39344|6|Mentioned|Map legend|Precambrian|Precambrian|Sturtian||||||
20468|Woocalla Dolomite Member|39724|6|Mentioned|Fig.6|||||||||
20468|Woocalla Dolomite Member|41405|3|Fully described|p166|||See also P194||||||
20468|Woocalla Dolomite Member|42235|4|Described|p139|||||||||
20468|Woocalla Dolomite Member|43052|5|Briefly described|p189,Table 6.1|||of Tapley Hill Formation||||||
20468|Woocalla Dolomite Member|43094|6|Mentioned|p35|||||||||
20468|Woocalla Dolomite Member|44538|4|Described|map legend|||(H53-16). Geol.Atlas Series. "Collenia" reef. Umberatana Group Equivalent. Sturtian.||||||
20468|Woocalla Dolomite Member|44934|5|Briefly described|Map Legend||Adelaidean|||||||
20468|Woocalla Dolomite Member|70082|6|Mentioned|p2|Cryogenian|Cryogenian|Stuart Shelf.||Unit of Tapley Hill Formation.||||
20468|Woocalla Dolomite Member|70334|6|Mentioned|p77|||Of Stuart Shelf. Marginal sandy and dolomitic facies deposited on the western margin of the basin.||||||
20468|Woocalla Dolomite Member|71129|5|Briefly described|p108|||Of Stuart Shelf.||||Correlable with Lincoln Member.||
20468|Woocalla Dolomite Member|72247|5|Briefly described|p39-43|Neoproterozoic|Neoproterozoic|Of Adelaide Geosyncline. Nomenclature originally of Johns et al. (1964).||||Overlain, and transitional to Tapley Hill Formation. Underlain by Gundon beds.||
20524|Woodnamoka Phyllite|22869|6|Mentioned|P46|||Correlated to the Carey Gully Sandstone Member||||||
20524|Woodnamoka Phyllite|22889|6|Mentioned|p31|Adelaidean|Adelaidean|Parent - Emeroo Subgroup.  Woodnamoka Phyllite of the northern Flinders Ranges.||||||
20524|Woodnamoka Phyllite|23394|5|Briefly described|Map legend|Proterozoic|Proterozoic|||||||
20524|Woodnamoka Phyllite|23411|6|Mentioned|Map Legend|||||||||
20524|Woodnamoka Phyllite|23818|5|Briefly described|p55|||Max. thickness: 4500 ft. Overlying unit: Blue Mine Conglomerate.||||||
20524|Woodnamoka Phyllite|24176|4|Described|p10, p25 Tb. 1|Adelaidean|Adelaidean|Of Callana Beds.  Silty phyllite, minor sandstone and sedimentary breccias at base.  Overlain by Blue Mine Conglomerate.  Age is Willouran.  Max. thickness: 1370m.  Geological Province: Mount Painter Province.||||||
20524|Woodnamoka Phyllite|24546|5|Briefly described|p2 - 3 Fig.2|Neoproterozoic|Neoproterozoic|Of Burra Group. Overlain by Blue Mine Conglomerate. Geological Province: Adelaide Fold Belt.||||||16-JAN-08
20524|Woodnamoka Phyllite|30176|6|Mentioned|Map legend|Adelaidean|Adelaidean|Willouran||||||
20524|Woodnamoka Phyllite|30177|2|Defined|p127|Adelaidean|Adelaidean|See also p60. Type section: East side of Wywyana Creek, lat. 30degrees 17'10"S  long. 139degrees21'00"E to lat. 30degrees 18'28"S  long. 139degrees21'03"E.||||||25-NOV-22
20524|Woodnamoka Phyllite|30801|6|Mentioned|p5|||Upper Callanna Beds. Table P5-6||||||
20524|Woodnamoka Phyllite|30807|6|Mentioned|p103|||Suggested map symbol||||||
20524|Woodnamoka Phyllite|32724|6|Mentioned|Fig.1|||Correlation. Willouran||||||
20524|Woodnamoka Phyllite|33474|6|Mentioned|Fig.4|||||||||
20524|Woodnamoka Phyllite|34535|5|Briefly described|p54|||U.Callanna Beds.||||||
20524|Woodnamoka Phyllite|35255|6|Mentioned|Fig.7|||||||||
20524|Woodnamoka Phyllite|36733|6|Mentioned|Table 5|||||||||
20524|Woodnamoka Phyllite|37854|6|Mentioned|Table 1|||||||||
20524|Woodnamoka Phyllite|38157|6|Mentioned|Table III|||||||||
20524|Woodnamoka Phyllite|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Torrensian||||||
20524|Woodnamoka Phyllite|39530|6|Mentioned|p139|||||||||
20524|Woodnamoka Phyllite|40294|6|Mentioned|p9|||||||||
20524|Woodnamoka Phyllite|41403|6|Mentioned|p43|||||||||
20524|Woodnamoka Phyllite|41404|3|Fully described|p86|||||||||
20524|Woodnamoka Phyllite|42222|6|Mentioned|Table 1 P5|||||||||
20524|Woodnamoka Phyllite|43052|5|Briefly described|p179,Table 6.1|||Of Emeroo Subgroup.||||||05-FEB-08
20524|Woodnamoka Phyllite|44133|6|Mentioned|p54|||||||||
20524|Woodnamoka Phyllite|65925|5|Briefly described|p124 Fig.3, p127.|||Subjected to amphibolite-facies metamorphism.||Unit in Burra Group.|||Phyllite, arkose, grit.|
20524|Woodnamoka Phyllite|70384|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Adelaide Geosyncline. Age shown more specifically as Willouran [Cryogenian].||Emeroo Subgroup.||Conformably? overlies Humanity Seat Formation. Is overlain ?conformably by Blue Mine Conglomerate.|Phyllite; sedimentary breccia; sandstone; arkose; argillaceous sandstone.|18-JAN-19
20551|Wooldridge Limestone Member|23818|6|Mentioned|p141 Fig.65|||Geological Province: Great Artesian Basin. Of the Oodnadatta Formation.||||||
20551|Wooldridge Limestone Member|23982|5|Briefly described|p58 Fig.18|||Of Oodnadatta Formation. Geological Province: Eromanga Basin.||||||
20551|Wooldridge Limestone Member|24092|5|Briefly described|p8 Fig.3|||Of Oodnadatta Formation. Geological Province: Eromanga Basin.||||||
20551|Wooldridge Limestone Member|24175|5|Briefly described|p17 Fig. 3|Albian|Albian|Appears to be misspelt?  Of Oodnatadatta Formation.  Geological Province: Eromanga Basin.||||||
20551|Wooldridge Limestone Member|30804|6|Mentioned|Table 2|||||||||
20551|Wooldridge Limestone Member|30807|6|Mentioned|p102|||Suggested map symbol||||||
20551|Wooldridge Limestone Member|32314|6|Mentioned|Fig. 4|||||||||
20551|Wooldridge Limestone Member|33017|6|Mentioned|p8|||||||||
20551|Wooldridge Limestone Member|33075|6|Mentioned|Table 1|||Refers Wopfner et al. (1970).||||||
20551|Wooldridge Limestone Member|33491|4|Described|p56|||Mention Fig.2||||||
20551|Wooldridge Limestone Member|33521|5|Briefly described|p8|||||||||
20551|Wooldridge Limestone Member|33819|6|Mentioned|p1|||||||||
20551|Wooldridge Limestone Member|33825|6|Mentioned|p10|||Correlation table||||||
20551|Wooldridge Limestone Member|33827|6|Mentioned|p13|||||||||
20551|Wooldridge Limestone Member|33828|6|Mentioned|p9|||Lithology||||||
20551|Wooldridge Limestone Member|33831|6|Mentioned|Map legend|Cenomanian|Neocomian|Neocomian - Cenomanian||||||
20551|Wooldridge Limestone Member|33832|6|Mentioned|p6|||Strat.||||||
20551|Wooldridge Limestone Member|33939|6|Mentioned|p386|||See also Fig.2||||||
20551|Wooldridge Limestone Member|33971|5|Briefly described|p37|||See also Fig.29.||||||
20551|Wooldridge Limestone Member|34611|6|Mentioned|p158|||Ammonites. See also Fig.65||||||
20551|Wooldridge Limestone Member|34725|6|Mentioned|p379|||||||||
20551|Wooldridge Limestone Member|36494|6|Mentioned|p148|||||||||
20551|Wooldridge Limestone Member|36571|6|Mentioned|p95|||See also P101, Table 4.||||||
20551|Wooldridge Limestone Member|38068|5|Briefly described|p72|||||||||
20551|Wooldridge Limestone Member|38199|6|Mentioned|p426|||||||||
20551|Wooldridge Limestone Member|38814|6|Mentioned|Table 1|||||||||
20551|Wooldridge Limestone Member|39211|5|Briefly described|Fig.6|||See also Figs 10-12,14-16 etc. Correlation||||||
20551|Wooldridge Limestone Member|40801|6|Mentioned|p73|||See also P85||||||
20551|Wooldridge Limestone Member|40925|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
20551|Wooldridge Limestone Member|40926|6|Mentioned|p17|||||||||
20551|Wooldridge Limestone Member|41012|3|Fully described|p143|||||||||
20551|Wooldridge Limestone Member|41064|6|Mentioned|p62|||||||||
20551|Wooldridge Limestone Member|41085|4|Described|p88|||||||||
20551|Wooldridge Limestone Member|41086|3|Fully described|p99|||||||||
20551|Wooldridge Limestone Member|41087|3|Fully described|p123|||||||||
20551|Wooldridge Limestone Member|41088|6|Mentioned|p141|||||||||
20551|Wooldridge Limestone Member|41117|5|Briefly described|p436|||||||||
20551|Wooldridge Limestone Member|41174|6|Mentioned|p117|||||||||
20551|Wooldridge Limestone Member|41266|6|Mentioned|Fig.3|||||||||
20551|Wooldridge Limestone Member|41523|5|Briefly described|p277|||||||||
20551|Wooldridge Limestone Member|41950|5|Briefly described|Fig.2 P3|||||||||
20551|Wooldridge Limestone Member|42746|6|Mentioned|Fig.6 P8|||||||||
20551|Wooldridge Limestone Member|44133|5|Briefly described|p104 Fig. 9.11, 122|||Geological Province: Eromanga Basin. Of the Oodnadatta Formation.||||||
20551|Wooldridge Limestone Member|44658|14|Not recorded|map legend|||Neocomian-Albian (G53-15).||||||
20551|Wooldridge Limestone Member|46937|6|Mentioned|Fig.10|||||||||
20551|Wooldridge Limestone Member|49010|6|Mentioned|Fig.4|||Eromanga Basin||||||
20551|Wooldridge Limestone Member|49011|6|Mentioned|Fig.3|||Eromanga Basin||||||
20551|Wooldridge Limestone Member|66529|6|Mentioned|p12 Fig.5|||||Unit in Oodnadatta Formation.||||
20551|Wooldridge Limestone Member|71321|6|Mentioned|p15|||Of Eromanga Basin.||||||
20551|Wooldridge Limestone Member|71863|5|Briefly described|p10|||Eromanga Basin. Also misspelt Wooldrige Limestone Member same page. Age would be Albian if equivalent to Toolebuc.||||Equivalent to the Toolebuc Formation.||01-MAY-19
20551|Wooldridge Limestone Member|72298|5|Briefly described|p801|Cretaceous|Cretaceous|Eromanga Basin (SA).||Oodnadatta FZ.||||
20586|Wooltana Volcanics|22553|6|Mentioned|p77,p83|||part of the Adelaidean sequence||||||
20586|Wooltana Volcanics|22631|6|Mentioned|p177|||||||||
20586|Wooltana Volcanics|22725|6|Mentioned|p246|Adelaidean|Neoproterozoic|Part of the Callanna Group.||||||18-APR-13
20586|Wooltana Volcanics|22772|4|Described|p65,Table13.1|Cryogenian|Cryogenian|Max Age: 800 Ma||||||
20586|Wooltana Volcanics|22857|5|Briefly described|Tb. 13.1 (insert p70-71), p65|Willouran|Willouran|Of the Arkaroola Subgroup (Callanna Group). Considered a correlative of Wilangee Basalt (NSW). Age: revised from 830+/-50Ma to ~800Ma (Cooper, 1975).||||||
20586|Wooltana Volcanics|23054|6|Mentioned|p11|||||||||
20586|Wooltana Volcanics|23282|6|Mentioned|p54|||Of Adelaide Fold belt and may be equivalent to Cadlareena Volcanics.||||||18-APR-13
20586|Wooltana Volcanics|23394|5|Briefly described|Map legend|Proterozoic|Proterozoic|||||||
20586|Wooltana Volcanics|23411|6|Mentioned|Map Legend|||||||||
20586|Wooltana Volcanics|23412|5|Briefly described|Map Legend|Proterozoic|Proterozoic|||||||
20586|Wooltana Volcanics|23557|6|Mentioned|p99|||||||||
20586|Wooltana Volcanics|23562|5|Briefly described|p295 Fig 2|Cryogenian|Cryogenian|Age: 827+/-6 Ma.||||||
20586|Wooltana Volcanics|23775|6|Mentioned|p723|||||||||22-SEP-09
20586|Wooltana Volcanics|23818|5|Briefly described|p36 Fig.9|Adelaidean|Adelaidean|Underlying unit: Wywyana Formation. Max. thickness: 2000 ft.||||||
20586|Wooltana Volcanics|24138|4|Described|p10 Fig. 1.1, p16|Precambrian|Precambrian|Basalt, andesite and trachyte. Geological Province: Adelaide Geosyncline.||||||
20586|Wooltana Volcanics|24175|6|Mentioned|p8|||||||||
20586|Wooltana Volcanics|24176|4|Described|p9, p26 Tb. 1|Adelaidean|Adelaidean|Of Callanna Beds.  Altered basalts, minor rhyolite and andesite, quartzites, tuffs, calc-silicate metasediments. Age is Willouran. Overlain by Humanity Seat Formation.  Max. thickness: >2400m.  Geological Province: Mount Painter Province.||||||06-FEB-08
20586|Wooltana Volcanics|24400|5|Briefly described|p155|Adelaidean|Adelaidean|Of Callanna Group. Overlain by Rook Tuff.||||||18-APR-13
20586|Wooltana Volcanics|24546|5|Briefly described|p2 - 3 Fig.2|Neoproterozoic|Neoproterozoic|Includes hornblende, plagioclase and epidote metabasalt. Overlies Wywyana Formation. Of Arkaroola Subgroup. Geological Province: Adelaide Fold Belt.||||||18-APR-13
20586|Wooltana Volcanics|24570|6|Mentioned|p400|||||||||
20586|Wooltana Volcanics|24593|5|Briefly described|p612 Fig. 1a|Adelaidean|Adelaidean|Of the Callana Group.  Geological Province: Mount Painter Inlier.  See also p613 Fig. 1b.||||||
20586|Wooltana Volcanics|24604|5|Briefly described|p907 Fig. 4|Neoproterozoic|Neoproterozoic|||||||
20586|Wooltana Volcanics|29656|6|Mentioned|p19|||||||||
20586|Wooltana Volcanics|30176|6|Mentioned|Map legend|Adelaidean|Adelaidean|Willouran||||||
20586|Wooltana Volcanics|30177|4|Described|p53|||See also P54-57||||||
20586|Wooltana Volcanics|30255|6|Mentioned|p217|||||||||
20586|Wooltana Volcanics|30261|6|Mentioned|Table 1|||Willouran age||||||
20586|Wooltana Volcanics|30376|5|Briefly described|p75|||See also P77||||||
20586|Wooltana Volcanics|30712|5|Briefly described|p58|||||||||
20586|Wooltana Volcanics|30801|6|Mentioned|p5|||Lower Callanna Beds. Table P5-6||||||
20586|Wooltana Volcanics|30807|6|Mentioned|p103|||Suggested map symbol||||||
20586|Wooltana Volcanics|31923|6|Mentioned|p8|||||||||
20586|Wooltana Volcanics|32722|6|Mentioned|p58|||||||||
20586|Wooltana Volcanics|32724|6|Mentioned|Fig.1|||Correlation||||||
20586|Wooltana Volcanics|32823|6|Mentioned|p364|||||||||
20586|Wooltana Volcanics|33004|6|Mentioned|p135|||||||||
20586|Wooltana Volcanics|33474|6|Mentioned|Fig.4|||||||||
20586|Wooltana Volcanics|33630|6|Mentioned|Table 1|||||||||
20586|Wooltana Volcanics|34267|5|Briefly described|p105|||||||||
20586|Wooltana Volcanics|34269|6|Mentioned|Table 1|||||||||
20586|Wooltana Volcanics|34534|6|Mentioned|Fig.2.13|||||||||
20586|Wooltana Volcanics|34535|5|Briefly described|p53|||||||||
20586|Wooltana Volcanics|34537|6|Mentioned|Fig.9|||||||||
20586|Wooltana Volcanics|34812|6|Mentioned|Table 8|||||||||
20586|Wooltana Volcanics|34834|6|Mentioned|p221|||||||||
20586|Wooltana Volcanics|35255|6|Mentioned|p7|||||||||
20586|Wooltana Volcanics|35270|6|Mentioned|Fig.2|||||||||
20586|Wooltana Volcanics|35320|6|Mentioned|p460|||Correlation||||||
20586|Wooltana Volcanics|35706|6|Mentioned|p11|||||||||14-MAY-07
20586|Wooltana Volcanics|36137|4|Described|p5|||Discussion re age.||||||
20586|Wooltana Volcanics|36198|6|Mentioned|p324|||||||||
20586|Wooltana Volcanics|36731|6|Mentioned|p123|||||||||
20586|Wooltana Volcanics|36733|6|Mentioned|p29|||||||||
20586|Wooltana Volcanics|37461|4|Described|p335|||||||||
20586|Wooltana Volcanics|37501|6|Mentioned|p415|||||||||
20586|Wooltana Volcanics|37818|6|Mentioned|p78|||||||||
20586|Wooltana Volcanics|37854|6|Mentioned|p8|||||||||
20586|Wooltana Volcanics|37931|6|Mentioned|p535|||||||||
20586|Wooltana Volcanics|38157|6|Mentioned|Table 1|||See also Table II.||||||
20586|Wooltana Volcanics|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Willouran||||||
20586|Wooltana Volcanics|39348|6|Mentioned|Map legend|Adelaidean|Adelaidean|Willouran||||||
20586|Wooltana Volcanics|39352|6|Mentioned|Map legend|Adelaidean|Adelaidean|Willouran||||||
20586|Wooltana Volcanics|39490|6|Mentioned|p10|||||||||
20586|Wooltana Volcanics|39635|6|Mentioned|Fig.2|||||||||
20586|Wooltana Volcanics|39885|6|Mentioned|p431|||||||||
20586|Wooltana Volcanics|40225|6|Mentioned|Map sheet|||||||||
20586|Wooltana Volcanics|40254|6|Mentioned|p285|||||||||
20586|Wooltana Volcanics|40294|6|Mentioned|p29|||See also P54||||||
20586|Wooltana Volcanics|40595|6|Mentioned|p77|||||||||
20586|Wooltana Volcanics|41401|6|Mentioned|p29|||||||||
20586|Wooltana Volcanics|41403|3|Fully described|p52|||||||||
20586|Wooltana Volcanics|41404|6|Mentioned|p86|||||||||
20586|Wooltana Volcanics|41405|6|Mentioned|p148|||||||||
20586|Wooltana Volcanics|41957|5|Briefly described|p67|||||||||
20586|Wooltana Volcanics|42098|5|Briefly described|Table 2 P54|||||||||
20586|Wooltana Volcanics|42167|6|Mentioned|Fig.2 P115|||||||||
20586|Wooltana Volcanics|42222|5|Briefly described|p11|||||||||
20586|Wooltana Volcanics|42224|6|Mentioned|Table 1 P53|||||||||
20586|Wooltana Volcanics|42238|6|Mentioned|Table 1 P74|||||||||
20586|Wooltana Volcanics|42246|6|Mentioned|p16|||||||||
20586|Wooltana Volcanics|42275|6|Mentioned|p478|||||||||
20586|Wooltana Volcanics|42760|6|Mentioned|p3|||||||||
20586|Wooltana Volcanics|42813|6|Mentioned|p14|||||||||
20586|Wooltana Volcanics|43052|5|Briefly described|p172, Table 6.1|||Of Arkaroola Subgroup.||||||03-FEB-09
20586|Wooltana Volcanics|43053|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Basalt. Diapiric carbonate-cemented breccia.||||||26-MAY-05
20586|Wooltana Volcanics|43086|6|Mentioned|p9|||||||||
20586|Wooltana Volcanics|43094|5|Briefly described|p33|||Of Callanna Group.||||||06-FEB-08
20586|Wooltana Volcanics|43258|5|Briefly described|Map Legend||Neoproterozoic|||||||
20586|Wooltana Volcanics|43298|5|Briefly described|Map Legend||Adelaidean|||||||
20586|Wooltana Volcanics|43383|14|Not recorded|p6|||||||||
20586|Wooltana Volcanics|43390|14|Not recorded|p10|||||||||
20586|Wooltana Volcanics|43560|6|Mentioned|p227|||||||||
20586|Wooltana Volcanics|43845|6|Mentioned|p43|||||||||12-JUL-16
20586|Wooltana Volcanics|45087|5|Briefly described|p102|||Chemical analyses||||||
20586|Wooltana Volcanics|60718|6|Mentioned|p49|||||Of Arkaroola Subgroup, Mount Painter Inlier.||Overlies Wywyana Formation.||15-APR-11
20586|Wooltana Volcanics|60953|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Basic volcanic rocks.||||||
20586|Wooltana Volcanics|60959|5|Briefly described|Map Legend|||||||||
20586|Wooltana Volcanics|61108|5|Briefly described|map legend|Adelaidean|Adelaidean|Basic volcanic rock.||||||
20586|Wooltana Volcanics|61238|6|Mentioned|p48|Neoproterozoic|Neoproterozoic|Age: 830 Ma.||||||14-MAY-07
20586|Wooltana Volcanics|61307|5|Briefly described|p5|||Of the Callanna Group. Geological Province: Adelaide Fold Belt.||||||18-APR-13
20586|Wooltana Volcanics|61412|6|Mentioned|p4 Fig.1||Neoproterozoic|||||||
20586|Wooltana Volcanics|61732|5|Briefly described|p36|||Top of the Callanna Group. Mafic lavas. Age: 827+/-6 Ma by correlation with Gairdner Dyke Swarm date from Stuart Shelf. Geological Province: Adelaide Rift Complex/Stuart Shelf.||||||17-SEP-13
20586|Wooltana Volcanics|62428|5|Briefly described|p351 Tb. 6|Neoproterozoic|Neoproterozoic|Age: 827+/-6Ma (SHRIMP U-Pb). Palaeomagnetic data.||||||10-FEB-09
20586|Wooltana Volcanics|62592|5|Briefly described|p50 Table 5.1, p57.|Willouran|Willouran|Adelaide Geosyncline.||Unit in Arkaroola Subgroup.||Overlies Wywyana Formation.|Mafic volcanics.|
20586|Wooltana Volcanics|62664|5|Briefly described|p137, pp138-139, pp150-151.|Neoproterozoic|Neoproterozoic|A c.2 km thick flood basalt sequence near the base of the Adelaide Geosyncline. Deformed and metamorphosed during Delamerian Orogeny.|830 +/- 50 Ma (Compston et al. 1966)|Unit in Arkaroola Subgroup.|||Sub-aerial tholeiitic continental flood basalts; dolerite and gabbro.|
20586|Wooltana Volcanics|62962|6|Mentioned|p2284 Fig. 2, p2287|Adelaidean|Adelaidean|Age: 827+/-6Ma. Geological Province: Mount Painter Province.||||||07-FEB-11
20586|Wooltana Volcanics|62993|5|Briefly described|p30|Neoproterozoic|Neoproterozoic|||Arkaroola Subgroup|||Mafic igneous and volcanic rocks.|
20586|Wooltana Volcanics|63022|6|Mentioned|p1018, p1019 Fig. 5|||Includes metabasalt.||||||
20586|Wooltana Volcanics|64625|6|Mentioned|p246, p258|||Adelaide Rift Complex. Probably fed by the Gairdner Dyke Swarm. Appears as Wooltana (Willouran) volcanics on p258.||||||
20586|Wooltana Volcanics|64647|6|Mentioned|p44, p46|Willouran|Willouran|||||||
20586|Wooltana Volcanics|64793|6|Mentioned|p284 Fig.3, p285  |||Mis-spelt as Wooltanna in Fig.3.||Unit in Arkaroola Subgroup.||Lateral equivalent of Beda Volcanics.||
20586|Wooltana Volcanics|64796|6|Mentioned|p183 fig 2, p184, p187, p189-190 Fig.7,8|Cryogenian|Cryogenian|Probably fed by Gairdner Dyke Swarm. Records the first major phase of Neoproterozoic crustal extension.|840-830 Ma.|Arkaroola Subgroup||Equivalent to Beda Volcanics.||
20586|Wooltana Volcanics|64797|6|Mentioned|p153 Fig.2|Cryogenian|Cryogenian|Adelaide Rift Complex. Lithology/rank not shown on diagram.||||||
20586|Wooltana Volcanics|65365|5|Briefly described|p10|Cryogenian|Cryogenian|Probably fed by the Gairdner Dyke Swarm. Possible correlative of Cadlareena Volcanics.||||||19-MAR-12
20586|Wooltana Volcanics|65369|5|Briefly described|p35, 36|||South Australian metabasalt. Thought to be correlative with the Gairdner Dyke Swarm and the Keene Basalt.||||||19-MAR-12
20586|Wooltana Volcanics|65925|5|Briefly described|p124 Fig.3, Appendix 2.|||||Unit in Arkaroola Subgroup.|||Metasediments; marble; trachyte; sandstone; schist; phyllite; basal conglomerate.|
20586|Wooltana Volcanics|67536|6|Mentioned|Map Legend||||||||Mafic volcanic rocks|
20586|Wooltana Volcanics|69019|6|Mentioned|p78, p80 Fig.17.|Neoproterozoic|Neoproterozoic|Mt Painter Inlier. Mentioned in comparison with Ooloo Hill Formation basalts which are chemically dissimilar.|c.830 Ma.|||||
20586|Wooltana Volcanics|69023|6|Mentioned|p64|||Poorly-constrained Rb-Sr age.|~830 Ma (Compston et al., 1966).|||||
20586|Wooltana Volcanics|69666|5|Briefly described|p24, p26, p33, p35-37|Neoproterozoic|Neoproterozoic|Part of the Willouran Basic Province. Bordering the Mount Painter Inlier, northern Flinders Ranges. Geochemistry described in some detail. Similar major and trace element abundances to Beda Basalt.|830 Ma.|Arkaroola Subgroup.||Correlated with Beda Basalt.||
20586|Wooltana Volcanics|70328|6|Mentioned|p160-162|Tonian|Tonian|Adelaide Geosyncline. Compositionally similar to Gairdner Dyke Swarm; suggested by Crawford and Hillyard (1990) to collectively form the "Willouran basic province' alongside Beda Volcanics.|830+\-50 Ma (Rb-Sr; Compston et al., 1966).|||||
20586|Wooltana 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).||||||
20586|Wooltana Volcanics|70384|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Adelaide Geosyncline. A sub-unit of red sandstone, shale and epidote quartzite interbeds is mapped separately. Age shown more specifically as Willouran [basal Cryogenian].||Arkaroola Subgroup.||Overlies Wywyana Formation.|Basalt lava, often amygdaloidal, deuterically altered or metamorphosed, red and purple; quartzite, heavy-mineral laminated, red or grey; shale and siltstone, red and purple; tuff; rare trachyte, calcareous metasediment.|18-JAN-19
20586|Wooltana Volcanics|70657|6|Mentioned|p50|||Adelaide Geosyncline.||||||
20586|Wooltana Volcanics|71001|6|Mentioned|p22|Tonian|Tonian||827 +/- 6 Ma.|||||
20586|Wooltana 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 Cadlareena 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).||||||
20586|Wooltana Volcanics|71237|14|Not recorded|p10|||||||||
20586|Wooltana Volcanics|71239|14|Not recorded|p5, 10|||||||||
20586|Wooltana Volcanics|72429|6|Mentioned|p975|||Mt Painter Province.||||||
20586|Wooltana Volcanics|73188|6|Mentioned|p315|||Accompanied earliest rifting in the Adelaide Geosyncline.||||||
20586|Wooltana Volcanics|73222|5|Briefly described|p6-7, p11, p16, p24|Tonian|Tonian|Adelaide Rift Complex, Gammon and Flinders ranges. Willouran. Geochron from Preiss (1987); sampled from Flinders Ranges.|827 +/- 6 to 830 +/- 50 Ma|Arkaroola Subgroup, Callanna Group, Warrina Supergroup||Underlain[?] by Wywyana Formation. Possibly equivalent to Noranda Volcanics.||
20586|Wooltana Volcanics|73262|6|Mentioned|p580|Tonian|Tonian|Geochron based on a Rb-Sr isochron (Compston et al., 1966).|ca 850 Ma|||Coeval with Gairdner Dyke Swarm.||
20586|Wooltana Volcanics|74367|5|Briefly described|p7 Fig.6, p8, p12, p18, p20|Tonian|Tonian|Willouran Basic Province. Age recalculated in Preiss (2000) from Compston et al., (1966). Correlative Gairdner Dolerite age of ca. 827 Ma has been quoted as the age of the Wooltana Volcanics (Hore, 2015; Keeman et al., 2020; Mackay, 2011).|830+/-50 Ma Rb-Sr whole rock|Arkaroola Subgroup||Unconformably underlies Burra Group, correlated with Gairdner Dolerite, Noranda Volcanics, Caldlareena Volcanics, Beda Basalt, Willangee Basalt, 'Depot Creek Volcanics'.||
20618|Woorinen Formation|2967|5|Briefly described|p54|||Lawrence (1966). Contains pelletal clay structures. Has an abnormally high carbonate content.||||Overlies Blanchetown Clay.|Aeolian. Has six palaeosols.|
20618|Woorinen Formation|10010|5|Briefly described|p11, p14 Fig. 5f|Late Pleistocene|Late Pleistocene|Geological Province: Murray Basin.Includes surficial deposits such as mobile sand sheets, source-bordering dunes and lunettes. See also p16.||||||13-AUG-07
20618|Woorinen Formation|22531|5|Briefly described|p22|Quaternary|Quaternary|||||||
20618|Woorinen Formation|22532|5|Briefly described|map legend|Quaternary|Quaternary|||||||
20618|Woorinen Formation|22799|2|Defined|p44|Holocene|Late Pleistocene|||||||
20618|Woorinen Formation|22857|5|Briefly described|p354|Quaternary|Quaternary|Geological Province: Murray Basin.||||||
20618|Woorinen Formation|22887|3|Fully described|p40|Late Pleistocene|Pleistocene|||||||
20618|Woorinen Formation|22893|3|Fully described|p45,46|Late Pleistocene|Pleistocene|||||||
20618|Woorinen Formation|23089|6|Mentioned|p649|||||||||
20618|Woorinen Formation|23252|5|Briefly described|Map Legend||Pleistocene|||||||
20618|Woorinen Formation|23402|5|Briefly described|p35|Quaternary|Quaternary|Geological Province: Adelaide Fold Belt||||||
20618|Woorinen Formation|23560|5|Briefly described|p150|||See also page 163.||||||
20618|Woorinen Formation|23818|5|Briefly described|p212 Fig.108|Late Pleistocene|Late Pleistocene|Geological Province: Great Artesian Basin and Murray Basin.||||||
20618|Woorinen Formation|23921|5|Briefly described|p1109 Table 1|Quaternary|Quaternary|Geological Province: Murray Basin.||||||
20618|Woorinen Formation|24439|6|Mentioned|p38|Quaternary|Quaternary|||||||
20618|Woorinen Formation|24551|5|Briefly described|p338 Fig. 11.2, 341|Holocene|Middle Pleistocene|Overlies Blanchetown Clay.||||||03-JUL-13
20618|Woorinen Formation|29898|6|Mentioned|p216|||||||||
20618|Woorinen Formation|30581|6|Mentioned|Map legend|Quaternary|Quaternary|||||||
20618|Woorinen Formation|30750|6|Mentioned|p4|||Reworked to form Bunyip Sands & Molineaux Sand||||||
20618|Woorinen Formation|30751|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
20618|Woorinen Formation|30752|6|Mentioned|p2|||See also P4,5.||||||
20618|Woorinen Formation|30753|4|Described|p15|Late Pleistocene||Upper Pleistocene age||||||22-JUL-09
20618|Woorinen Formation|30754|2|Defined|Appendix 1|late Pleistocene|late Pleistocene|See also Table 22, P35,38,41||||||
20618|Woorinen Formation|30755|6|Mentioned|p169|||Tectonic map||||||
20618|Woorinen Formation|30756|6|Mentioned|p4|||||||||
20618|Woorinen Formation|30807|6|Mentioned|p101|||Suggested map symbol||||||
20618|Woorinen Formation|30934|6|Mentioned|Map legend|Pliocene|Pliocene|||||||
20618|Woorinen Formation|30935|6|Mentioned|Map legend|Recent|Recent|||||||
20618|Woorinen Formation|30936|6|Mentioned|Map legend|Pliocene|Pliocene|||||||
20618|Woorinen Formation|30994|6|Mentioned|p250|||Palacosals [?palaeosols] discussed.||||||03-JUL-13
20618|Woorinen Formation|30996|6|Mentioned|p42|||||||||
20618|Woorinen Formation|31345|6|Mentioned|p293|||||||||
20618|Woorinen Formation|31741|6|Mentioned|p6|||||||||
20618|Woorinen Formation|31745|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
20618|Woorinen Formation|31747|6|Mentioned|Map legend|Quaternary|Quaternary|||||||
20618|Woorinen Formation|32426|6|Mentioned|p141|||Loose sand||||||
20618|Woorinen Formation|32861|5|Briefly described|Table 1|||||||||
20618|Woorinen Formation|33725|6|Mentioned|p9|||Small sinkholes||||||
20618|Woorinen Formation|33767|6|Mentioned|Fig.5|||||||||
20618|Woorinen Formation|33826|6|Mentioned|p42|||Strat. table||||||
20618|Woorinen Formation|34180|5|Briefly described|p217|Late Pleistocene||Upper Pleistocene||||||22-JUL-09
20618|Woorinen Formation|34459|5|Briefly described|p11|Recent||Recent||||||22-JUL-09
20618|Woorinen Formation|34536|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
20618|Woorinen Formation|34735|4|Described|p45|||Also mention P35.||||||
20618|Woorinen Formation|34758|6|Mentioned|Fig.2|||||||||
20618|Woorinen Formation|34954|5|Briefly described|p199|||||||||
20618|Woorinen Formation|35012|6|Mentioned|p430|||||||||
20618|Woorinen Formation|35071|6|Mentioned|Fig.4|||||||||
20618|Woorinen Formation|35097|6|Mentioned|Fig.4|||||||||
20618|Woorinen Formation|35131|6|Mentioned|p10|||||||||
20618|Woorinen Formation|35200|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
20618|Woorinen Formation|35232|5|Briefly described|Table.4|||||||||
20618|Woorinen Formation|35272|3|Fully described|p285|||||||||
20618|Woorinen Formation|35274|6|Mentioned|p425|||||||||
20618|Woorinen Formation|37873|4|Described|p3|||||||||
20618|Woorinen Formation|38068|6|Mentioned|Fig.8|||Murray Basin||||||
20618|Woorinen Formation|38383|6|Mentioned|Table 1|||||||||
20618|Woorinen Formation|38601|6|Mentioned|p7|||||||||
20618|Woorinen Formation|40215|6|Mentioned|p56|||||||||
20618|Woorinen Formation|40380|6|Mentioned|p222|||||||||
20618|Woorinen Formation|41848|4|Described|p360|||||||||
20618|Woorinen Formation|41868|6|Mentioned|p579|||||||||
20618|Woorinen Formation|42125|6|Mentioned|p139|||||||||
20618|Woorinen Formation|42134|4|Described|p339|||||||||
20618|Woorinen Formation|42136|4|Described|Table 1 P364|||||||||
20618|Woorinen Formation|42264|6|Mentioned|p13|||||||||
20618|Woorinen Formation|42635|5|Briefly described|p94|||||||||
20618|Woorinen Formation|42717|5|Briefly described|map legend|Pleistocene||||||||
20618|Woorinen Formation|42720|5|Briefly described|map legend|Pleistocene||||||||
20618|Woorinen Formation|42827|3|Fully described|p360|||see also Table 9.1||||||
20618|Woorinen Formation|42966|1|Redefined|p229|Late Pleistocene||||||||
20618|Woorinen Formation|43053|5|Briefly described|Map Legend|Quaternary|Quaternary|||||||25-MAY-05
20618|Woorinen Formation|43073|4|Described|p18,Table 4|||||||||
20618|Woorinen Formation|43218|4|Described|Fig.3,p22||Quaternary|||||||
20618|Woorinen Formation|43258|5|Briefly described|Map Legend|Holocene|Pleistocene|||||||
20618|Woorinen Formation|43627|6|Mentioned|p6||Recent|Includes dune formations.||||||28-OCT-04
20618|Woorinen Formation|43655|5|Briefly described|p40-846|||||||||
20618|Woorinen Formation|43669|4|Described|p23||Pleistocene|||||||
20618|Woorinen Formation|44133|5|Briefly described|p253|Holocene|Middle Pleistocene|Geological Province: Murray Basin. Includes: Piangil Member, Kyalite Member, Speewa Member, Bymue Member, Miralie Member.||||||
20618|Woorinen Formation|44188|5|Briefly described|Map Legend||Pleistocene|Geological province: Murray Basin. Unconsolidated red-brown, siliceous, silty sand, red calcareous silty clay, sandy clay, clay pellet aggregates.||||||15-MAY-08
20618|Woorinen Formation|44191|5|Briefly described|Map Legend|Holocene|Early Pleistocene|||||||
20618|Woorinen Formation|46802|6|Mentioned|Table 1|||||||||
20618|Woorinen Formation|46909|6|Mentioned|Fig.2|||||||||
20618|Woorinen Formation|49038|5|Briefly described|p32|||||||||
20618|Woorinen Formation|60005|5|Briefly described|Map legend|Pleistocene|Pleistocene|Aeolian: dune sand, calcareous, clayey, palaesols.||||||03-JUL-13
20618|Woorinen Formation|60543|5|Briefly described|Map legend|Quaternary|Quaternary|Wind blown sand in east west dunes.||||||23-DEC-09
20618|Woorinen Formation|60953|5|Briefly described|Map Legend|Holocene|Pleistocene|Aeolian sand of inland dune fields. Includes associated alluvial and regolith materials in interdunal areas.||||||
20618|Woorinen 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.||||||
20618|Woorinen Formation|61155|5|Briefly described|p18|Pleistocene|Pleistocene|Overlies Blanchetown Clay. Age: <2.0Ma. Geological Province: Murray Basin.||||||
20618|Woorinen Formation|61181|5|Briefly described|p137|Recent|Pleistocene|Aeolian deposits containing calcrete (also known as kunkar or caliche). The calcrete sheets consist of light coloured concretionary calcite and minor dolomite.||||||
20618|Woorinen Formation|61207|5|Briefly described|p280 Fig. 2|Quaternary|Quaternary|Longitudinal dune sediments. Geological Province: Murray Basin.||||||
20618|Woorinen Formation|61964|3|Fully described|p14 Fig. 4, p168-171|Quaternary|Quaternary|Preceded by "The Featureless Sandplain". Now overlies this. Aeolian deposits of red-brown to light brown humic, clayey to silty, unconsolid' fine- to med.-grained quartz-lithic sand + red clay cutans. Over Blanchetown Clay in SW. Deposited: 0.7Ma-0.4Ma||||||
20618|Woorinen Formation|62405|5|Briefly described|Map legend|Quaternary|Quaternary|Aeolian-derived. Fossil dunefields of openly spaced, E-W linear dunes; red-brown to light brown humic, clayey to silty, fine- to med.-grained sand with red clay cutans, silty clay at depth; abundant pedogenic carbonate; extensively modified by pedogenesis||||||
20618|Woorinen Formation|65552|5|Briefly described|p2, p5 Fig 3, p6-7, p17, p27 App. 6|Quaternary|Quaternary|Aeolian deposits formed mainly in the late Pleistocene with minor Holocene reworking. A source of silica sands.||||||
20618|Woorinen Formation|66002|5|Briefly described|p13 Tb.9|Neogene|Neogene|Defined by Lawrence 1966.||||||
20618|Woorinen Formation|66012|5|Briefly described|p23|Quaternary|Quaternary|Aeolian. Possible correlative of Windgelli Clay|| ||||13-JUN-13
20618|Woorinen Formation|66287|5|Briefly described|p42, Fig 4-5,8|Holocene|Pleistocene|Forms parabolic and blow-out dune systems.||||Overlies the Bakara Soil.||20-APR-12
20618|Woorinen Formation|68116|5|Briefly described|Appendix, Maps 1-11, 14, 15, 22.|Holocene|Pleistocene|Forms discontinuous chains of east-west longitudinal dunes.|||||Dune deposits, unconsolidated; mainly red-brown siliceous silty sand, red calcareous silty clay, and sandy clay; calcareous nodules and palaeosols common; uppermost unit is mainly sand without calcareous nodules and clay matrix.|
20618|Woorinen Formation|68189|6|Mentioned|p30|Quaternary|Quaternary|||||||
20618|Woorinen Formation|68194|5|Briefly described|p19, p21, p24, p28, p71|Quaternary|Quaternary|Lawrence (1966). Is derived from local vertical weathering of Parilla Sand. Forms low longitudinal NE-SW dunes.|||Includes Piangil Member.|Unconformably overlies Parilla Sand and Shepparton Formation.|Aeolian sands: subangular to subrounded, fine- to medium-grained, iron-stained quartz grains with or without a red clay matrix.|
20618|Woorinen Formation|68716|6|Mentioned|p39 Fig.3|||||||Underlain by the Blanchetown Clay.||
20618|Woorinen Formation|69161|5|Briefly described|Map legend|Quaternary|Quaternary|Fossil dunefields of open-spaced, east-west linear (aeolian) dunes.|||||Red-brown to light-brown humic, clayey to silty, fine- to medium-grained sand with red clay cutans, silty clay at depth; abundant regolithic and pedogenic carbonate; extensively modified by pedogenesis.|
20618|Woorinen Formation|69162|5|Briefly described|Map legend|Quaternary|Quaternary|Fossil dunefields of open-spaced, east-west linear (aeolian) dunes.|||||Red-brown to light-brown humic, clayey to silty, fine- to medium-grained sand with red clay cutans, silty clay at depth; abundant regolithic and pedogenic carbonate; extensively modified by pedogenesis.|
20618|Woorinen Formation|69163|5|Briefly described|Map legend|Quaternary|Quaternary|Fossil dunefields of open-spaced, east-west linear (aeolian) dunes.|||||Red-brown to light-brown humic, clayey to silty, fine- to medium-grained sand with red clay cutans, silty clay at depth; abundant regolithic and pedogenic carbonate; extensively modified by pedogenesis.|
20618|Woorinen Formation|69164|5|Briefly described|Map legend|Quaternary|Quaternary|Fossil dunefields of open-spaced, east-west linear (aeolian) dunes.|||||Red-brown to light-brown humic, clayey to silty, fine- to medium-grained sand with red clay cutans, silty clay at depth; abundant regolithic and pedogenic carbonate; extensively modified by pedogenesis.|
20618|Woorinen Formation|70961|14|Not recorded|p136|||Section through east-west dune.||||||
20618|Woorinen Formation|72445|5|Briefly described|App.1, App.2.||Pliocene|App.2 is a .csv format file. Fine to medium sand in Stavely 04, 05, 07. Medium sand in Stavely 08. Silty sand (soil profile) in Stavely 11. Subangular to subrounded sandy mud in Stavely 14. Max age from underlying units.||||Overlies Calivil Formation (gradational contact), Loxton Sand (sharp contact).|Includes sandstone, mud and siltstone.|
20618|Woorinen Formation|73112|5|Briefly described|Map legend.|Pleistocene|Pleistocene|This unit is called the Woorinen Formation Equivalent in the map legend.|||||Pale brown aeolian calcareous silt-sand sheet containing carbonate of Loveday Soil.|
20618|Woorinen Formation|73118|6|Mentioned|p20|||||||Overlies Loxton-Parilla Sands.||
20618|Woorinen Formation|73496|5|Briefly described|Map legend|Pleistocene|Pleistocene||||||Wind blown silty sand in east-west linear dunes; no detectable magnetic response; radiometric response low in all channels.|
20618|Woorinen Formation|73505|5|Briefly described|p2, p12-13, p37|Quaternary|Quaternary|Murray Basin. Conformably overlies other units. Topography of convex-west arcuate dunes. Patchy low radiometric response from K, Th. No detectable magnetic response.|||||Windblown sand and silt.|
20650|Wright Hill Formation|23818|6|Mentioned|p56|||||||||
20650|Wright Hill Formation|30807|6|Mentioned|p103|||Suggested map symbol||||||
20650|Wright Hill Formation|31457|6|Mentioned|p11|||||||||
20650|Wright Hill Formation|31965|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
20650|Wright Hill Formation|34535|5|Briefly described|p56|||||||||
20650|Wright Hill Formation|41751|6|Mentioned|p8|||||||||
20650|Wright Hill Formation|62453|6|Mentioned|p50|||Underlies Punkerri Sandstone disconformably.||||||
20650|Wright Hill Formation|65102|4|Described|p365,366 Fig. 4-41; p.372, Table 4-15|Neoproterozoic|Neoproterozoic|Officer Basin. Laterally equivalent to Madley and Browne Formations. 500-3400m, siltstone, sandstone, quartzite; minor black oolitic chert; shallow marine; conformably overlying Pindyin beds (S.A.), type section in S.A., Birksgate and Lindsay areas, 27deg 35min S, 131deg 00min E; unfossiliferous.||||||
20650|Wright Hill Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone|
20668|Wundowie Limestone Member|22510|5|Briefly described|p39, table1|||Originally defined as part of Angepena Formation, then Etina Formation, now reassigned to Enorama Shale.||||||
20668|Wundowie Limestone Member|23394|5|Briefly described|Map legend|Proterozoic|Proterozoic|||||||
20668|Wundowie Limestone Member|24175|6|Mentioned|p13|||Of Etina Formation.||||||
20668|Wundowie Limestone Member|24321|5|Briefly described|Map legend|Adelaidean|Adelaidean|Parent: Etina Formation||||||
20668|Wundowie Limestone Member|30177|2|Defined|p131|Adelaidean|Adelaidean|See also p83. Type section: 9.7 miles south-southwest of Arkaroola Homestead, west side of Arkaroola Track, lat. 30degrees27'43"S long. 139degrees 18'47"E to lat. 30degrees27'49"S long. 139degrees 18'55"E.||Angepena Formation|||Three bands of pale grey or white weathering massive grey algal limestone, separated by red silty shales and siltstones and minor grey-green silty shales; locally gritty.|25-NOV-22
20668|Wundowie Limestone Member|30801|6|Mentioned|p5|||Table P5-6. Angepena Formation.||||||08-JUL-13
20668|Wundowie Limestone Member|30807|6|Mentioned|p103|||Suggested map symbol||||||
20668|Wundowie Limestone Member|32723|6|Mentioned|p101|||See also P107,110||||||
20668|Wundowie Limestone Member|32724|4|Described|p520|||Marinoan||||||
20668|Wundowie Limestone Member|32726|6|Mentioned|p189|||Stromatolites||||||
20668|Wundowie Limestone Member|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Marinoan||||||
20668|Wundowie Limestone Member|41405|4|Described|p182|||||||||
20668|Wundowie Limestone Member|42222|6|Mentioned|p17|||||||||
20668|Wundowie Limestone Member|43052|5|Briefly described|p189,Table 6.1|||||||||
20668|Wundowie Limestone Member|60718|5|Briefly described|p49 Fig. 2|Adelaidean|Adelaidean|Geological Province: Adelaide Geosyncline.||Of Amberoona Formation (Upalinna Subgroup, Umberatana Group).||||15-APR-11
20668|Wundowie Limestone Member|61732|5|Briefly described|p28 Fig. 13|Marinoan|Marinoan|Of the Enorama Shale (Upalinna Subgroup, Umberatana Group). Geological Province: Adelaide Rift Complex.||||||07-FEB-11
20668|Wundowie Limestone Member|64801|5|Briefly described|p110 Fig.2, p111, p116-117|Neoproterozoic|Neoproterozoic|Adelaide Rift Complex.||Enorama Shale.|||Includes columnar stromatolites (Tungussia etina).|
20668|Wundowie Limestone Member|64846|5|Briefly described|p198 Fig.3, p199 Fig.4, p202 Tb.1  |Cryogenian|Cryogenian|See also p203, p208 Fig.10.||Of the Enorama Shale.||||
20668|Wundowie Limestone Member|65493|5|Briefly described|p917, 924, p909 Fig 2, p920 Fig 12|Cryogenian|Cryogenian|Limestone member of the Enorama Shale (Preiss et al 1998). Previously defined as part of the Angepena Formation. Consists of three basin-wide stromatolite horizons.||||||
20668|Wundowie Limestone Member|67180|4|Described|p602 Fig.2, p606, Fig.7|Cryogenian|Cryogenian|Identified as 3 thin but very distinct stromatolitic limestone beds variously shown as Wundowie Limestone #1, #2 and #3, Wundowie Stromatolite Beds 1, 2, 3. Marinoan age. Previously of the Angepena Formation (Coats and Blisset 1971).||Unit in Enorama Shale.||Beds occur towards the base of the Enorama Shale.|Columnar and branching stromatolites, calcareous/dolomitic shale.|
20668|Wundowie Limestone Member|67979|4|Described|p536, p531 Fig.2, p534 Fig.5, p541-543|Marinoan|Marinoan|In the Northern Flinders Ranges, the unit is regionally recognised base of Enorama Shale (as defined by Coats and Blissett 1971), but shown above base in Fig.5. Occurs as 2-3 m-thick limestone beds interbedded within host calcareous shales.||Base of Enorama Shale||Conformably overlies Amberoona Formation in Northern Flinders Ranges; erosionally overlies Etina Formation in Central Flinders Ranges.|Sandy and stromatolitic limestones.|22-SEP-14
20668|Wundowie Limestone Member|70384|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Adelaide Geosyncline. Age shown more specifically as Marinoan [Cryogenian].||Of Enorama Shale.|||Gritty limestone with stromatolite bioherms, oolitic, clay pellets; dark grey calcareous siltstone laminations.|23-JAN-19
20668|Wundowie Limestone Member|72601|6|Mentioned|p19|Cryogenian|Cryogenian|Adelaide Rift Complex.||Enorama Shale, Umberatana Group||||
20670|Wunghnu Group|2967|6|Mentioned|p15 Fig.2.2||||||Calivil, Shepparton Formations.|Overlies Renmark Group. Is interbedded with Murray Group.||
20670|Wunghnu Group|10010|5|Briefly described|p12 Fig. 3|Pleistocene|Late Miocene|Geological Province: Murray Basin.||||||13-AUG-07
20670|Wunghnu Group|22756|6|Mentioned|P31|||||||||
20670|Wunghnu Group|22773|6|Mentioned|Fig24.8p352,354|||||||||
20670|Wunghnu Group|22799|5|Briefly described|p24 Fig.10|Pliocene|Pliocene|||||||
20670|Wunghnu Group|22857|5|Briefly described|p352 Fig.24.8, p354|Quaternary|Late Miocene|Includes the Shepparton, Torrumbarry and Calivil Formations. Geological Province: Murray Basin.||||||
20670|Wunghnu Group|23884|5|Briefly described|p155 Fig. 13.2|Pliocene|Late Miocene|Geological Province: Murray Basin.||||||21-SEP-09
20670|Wunghnu Group|24105|5|Briefly described|p158, 159|||Geological Province: Murray Basin. Underlain by Renmark Group.||||||09-OCT-08
20670|Wunghnu Group|24551|5|Briefly described|p320, p322 Fig. 10.29, p324|Pliocene|Late Miocene|Overlies Murray Group beds unconformably.||||||
20670|Wunghnu Group|29591|6|Mentioned|Table 20|||||||||
20670|Wunghnu Group|29898|6|Mentioned|p213|||||||||
20670|Wunghnu Group|31741|6|Mentioned|p6|||||||||
20670|Wunghnu Group|31746|5|Briefly described|p197|||||||||
20670|Wunghnu Group|32021|4|Described|p41|||||||||
20670|Wunghnu Group|32315|6|Mentioned|Fig. 2|||||||||
20670|Wunghnu Group|34735|4|Described|p36|||||||||
20670|Wunghnu Group|35091|6|Mentioned|p7|||Refers Lawrence (1966).||||||
20670|Wunghnu Group|35272|6|Mentioned|p276|||||||||
20670|Wunghnu Group|35285|5|Briefly described|p414|||||||||
20670|Wunghnu Group|35498|6|Mentioned|Fig.1|||||||||
20670|Wunghnu Group|37873|6|Mentioned|p3|||||||||
20670|Wunghnu Group|38293|4|Described|Table 1|||||||||
20670|Wunghnu Group|40795|5|Briefly described|p80|||||||||
20670|Wunghnu Group|41848|5|Briefly described|p352|Quaternary|Tertiary|The Shepparton Formation and Coonambidgal Formation constitute the upper part of this Group||||||
20670|Wunghnu Group|41868|6|Mentioned|p551|||||||||
20670|Wunghnu Group|42125|6|Mentioned|Fig.5 P132|||||||||
20670|Wunghnu Group|42130|6|Mentioned|Fig.3 P265|||||||||
20670|Wunghnu Group|42134|6|Mentioned|Fig.3 P335|||||||||
20670|Wunghnu Group|42137|6|Mentioned|Fig.2 P368|||||||||
20670|Wunghnu Group|42138|6|Mentioned|Fig.2 P390|||||||||
20670|Wunghnu Group|42827|5|Briefly described|p352|||see also Fig 9.1||||||
20670|Wunghnu Group|42881|4|Described|Fig.3, P84|||||||||
20670|Wunghnu Group|42966|2|Defined|p179|Quaternary|Late Miocene|||||||
20670|Wunghnu Group|43780|5|Briefly described|p6|||||||||
20670|Wunghnu Group|43791|6|Mentioned|p372, Fig1|||||||||
20670|Wunghnu Group|43804|6|Mentioned|Fig.2,p49|||||||||
20670|Wunghnu Group|44093|5|Briefly described|p145 App. 1|Tertiary|Tertiary|Geological Province: Kanmantoo Fold Belt.||||||
20670|Wunghnu Group|50156|5|Briefly described|Map Legend|Pleistocene|Miocene|Includes Shepparton Formation||||||
20670|Wunghnu Group|50157|5|Briefly described|Map Legend|Pleistocene|Miocene|Includes Shepparton Formation||||||
20670|Wunghnu Group|50158|5|Briefly described|Map Legend|Pleistocene|Miocene|Includes Shepparton Formation||||||
20670|Wunghnu Group|50159|5|Briefly described|Map Legend|Pleistocene|Miocene|Includes Shepparton Formation||||||
20670|Wunghnu Group|50160|5|Briefly described|Map Legend|Quaternary|Miocene|||||||16-JUN-04
20670|Wunghnu Group|50161|5|Briefly described|Map Legend|Pleistocene|Miocene|Includes Shepparton Formation||||||
20670|Wunghnu Group|50162|5|Briefly described|Map Legend|Pleistocene|Miocene|Includes Shepparton Formation||||||
20670|Wunghnu Group|50163|5|Briefly described|Map Legend|Pleistocene|Miocene|Includes Shepparton Formation||||||22-JUN-04
20670|Wunghnu Group|60451|6|Mentioned|p95|||||||||
20670|Wunghnu Group|60492|5|Briefly described|Map Legend|Pleistocene|Pliocene|Includes: Shepparton Formation.||||||
20670|Wunghnu Group|60599|4|Described|p85|Tertiary|Tertiary|Includes the Tertiary Calivil Formation and Torrumbarry Clay, and the Quaternary Shepparton and Coonambidgal Formations. Geological Province:Murray Basin.||||||14-JAN-09
20670|Wunghnu Group|61163|4|Described|p29, p101-102|Pleistocene|Pliocene|Comprises Calivil and Shepparton Formations. Geological Province: Lachlan Fold Belt.||||||
20670|Wunghnu Group|61174|5|Briefly described|map legend|Quaternary |Quaternary|Includes Shepparton Formation and Calivil Formation.||||||07-FEB-11
20670|Wunghnu Group|61175|5|Briefly described|map legend|Quaternary |Quaternary|Includes Shepparton Formation and Calivil Formation.||||||
20670|Wunghnu Group|61176|5|Briefly described|map legend|Quaternary |Quaternary|Includes Shepparton Formation and Calivil Formation.||||||
20670|Wunghnu Group|61177|5|Briefly described|map legend|Quaternary |Quaternary|Includes Shepparton Formation and Calivil Formation.||||||
20670|Wunghnu Group|61178|5|Briefly described|map legend|Quaternary |Quaternary|Includes Shepparton Formation.||||||
20670|Wunghnu Group|61185|5|Briefly described|p57|Quaternary|Tertiary|Of Lawrence (1966) including Calivil Sand, Turrumbarry Clay, Shepparton Formation and Coonambidgal Formation. Geological Province: Murray Basin.||||||07-FEB-11
20670|Wunghnu Group|61314|5|Briefly described|p129|Pleistocene|Pleistocene|Includes the Bungunnia Limestone. Geological Province: Murray Basin.||||||
20670|Wunghnu Group|61964|5|Briefly described|p139|Pliocene|Pliocene|Includes Shepparton Formation. Geological Province: Murray Basin.||||||
20670|Wunghnu Group|65552|5|Briefly described|p5 Fig. 3|Quaternary|Late Miocene|Upper (eastern) Murray Basin unit. Contains Shepparton and Calivil Formations, and Torrumbarry Clay. Unconformably overlies Renmark Group.||||||
20670|Wunghnu Group|65715|5|Briefly described|p11 Tb.7, p15 Tb.8|Neogene|Neogene|Includes Loxton Sand and Shepparton Formation. No longer includes Calivil Formation, which is considered older.||||||06-FEB-15
20670|Wunghnu Group|66002|5|Briefly described|p10 Tb.7, p13 Tb.9, p18|Neogene|Neogene|Includes Loxton Sand, Shepparton Formation. Previously included Calivil Formation.||||||27-MAY-13
20670|Wunghnu Group|66934|6|Mentioned|Map legend|Pliocene|Pliocene||||Includes Loxton-Parilla Sands.|||
20670|Wunghnu Group|68194|5|Briefly described|p22-24||Miocene|Lawrence (1966); Lawrence and Abeles (1988). Murray Basin. Deposition occurred during a final marine transgression that started in Late Miocene or Early Pliocene.|||Includes Bookpurnong beds, Parilla Sand, Karoonda Surface, Blanchetown Clay, Shepparton Formation, Yando Clay.|||
20670|Wunghnu Group|69798|5|Briefly described|p4 Fig.2|Pliocene|Pliocene|Murray Basin.|||Shepparton, Calivil Formations.|||
20670|Wunghnu Group|70718|5|Briefly described|p104||||||Includes the Loxton Sand and the Shepparton Formation.|||
20670|Wunghnu Group|70961|14|Not recorded|p136|||Refers to Lawrence (1966).||||||
20670|Wunghnu Group|72445|5|Briefly described|App1, App2; App.5; App.7 p7 Fig.4.|Pliocene|Late Miocene|Shown on the 'Lithostratigraphy of Cenozoic sediments in the Murray Basin' (from Brown & Stephenson 1991). App.2 is a .csv format file. Identified in Stavely 01,05,06,08,09,10, 11,12,14,16.|||Includes Loxton Sand, Calivil Formation, Torrumbarry Clay and Shepparton Formation.|Overlies Renmark, Heytesbury, Murray Groups, gradational/sharp contacts. Unconformably underlies Newer Volcanic Group. Shown as partial equivalent to Loxton-Parilla Sands, Blanchetown Clay.|Includes Silty sand to silty mud. Dominantly fine sand in Stavely01.|
20670|Wunghnu Group|73118|6|Mentioned|p81||||||Shepparton, Calivil Formations.|||
20670|Wunghnu Group|73496|5|Briefly described|Map legend|Holocene|Miocene||||Coonambidgal Formation, Blanchetown Clay, Shepparton Formation, Parilla Sand|||
20670|Wunghnu Group|73497|5|Briefly described|Map legend|Pleistocene|Neogene||||Calivil Formation, Parilla Sand, Shepparton Formation|||
20670|Wunghnu Group|73505|5|Briefly described|p13, p36|Pliocene|Late Miocene|Misspelt as Whungnu Group p11.|||Bookpurnong beds, Parilla Sand, Shepparton Formation, Blanchetown Clay|||
20695|Wyandra Sandstone Member|12597|5|Briefly described|p492 Tb.1, p499|Barremian|Early Cretaceous|E Eromanga Basin. Up to 60m thick. Forms the youngest pressurised aquifer in the Basin.||Unit in Cadna-owie Formation.|||Fine- to coarse-grained quartzose to sub-labile sandstone, pebbly in part, generally well sorted, porous and permeable; with minor siltstone interbeds towards the top.|
20695|Wyandra Sandstone Member|13516|5|Briefly described|p167 fig 10, p169 fig 11, p171 fig 12|Early Cretaceous|Early Cretaceous|In Eromanga Basin.||Of Cadna-owie Formation||||
20695|Wyandra Sandstone Member|22883|5|Briefly described|P31, Fig2||Early Cretaceous|Overlying unit is Bulldog Shale, underlying unit is Murta Formation, parent is Cadna-owie Formation||||||
20695|Wyandra Sandstone Member|22912|5|Briefly described|33|||Geol province Eromanga Basin.||||||16-SEP-08
20695|Wyandra Sandstone Member|23375|4|Described|Fig2 p265,267,269,271,277,279|Barremian|Hauterivian|Of the Cadna-owie Formation. In the Eromanga Basin.||||||17-JAN-08
20695|Wyandra Sandstone Member|23430|4|Described|p524 Table 14.7|||Of Cadna-owie Formation. Eromanga Basin Province.||||||
20695|Wyandra Sandstone Member|23982|5|Briefly described|p57|Cretaceous|Jurassic|Of the Cadna-owie Formation.  Geological Province: Eromanga Basin.||||||18-JUL-14
20695|Wyandra Sandstone Member|24092|5|Briefly described|p8 Fig.3|||Geological Province: Eromanga Basin.||||||
20695|Wyandra Sandstone Member|24210|5|Briefly described|p133 Fig. 2|Early Cretaceous|Early Cretaceous|Of the Cadna-owie Formation.  Geological Province: Eromanga Basin.||||||
20695|Wyandra Sandstone Member|24482|5|Briefly described|p44|Cretaceous|Jurassic|Of the Cadna-owie Formation. Geological Province: Eromanga Basin.||||||
20695|Wyandra Sandstone Member|32314|6|Mentioned|Fig. 4|||||||||
20695|Wyandra Sandstone Member|33017|6|Mentioned|Table 1|||||||||
20695|Wyandra Sandstone Member|33075|2|Defined|p452|Early Cretaceous|Early Cretaceous|||||||
20695|Wyandra Sandstone Member|33086|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
20695|Wyandra Sandstone Member|35239|6|Mentioned|p265|||||||||
20695|Wyandra Sandstone Member|35663|6|Mentioned|Fig.2|||Subsurface correlations of the central basin rock units.||||||
20695|Wyandra Sandstone Member|36251|6|Mentioned|Fig.2|||||||||
20695|Wyandra Sandstone Member|36571|6|Mentioned|Table 4|||||||||
20695|Wyandra Sandstone Member|38226|6|Mentioned|Table 1|||See also Fig.6.||||||
20695|Wyandra Sandstone Member|39070|4|Described|p364|||||||||
20695|Wyandra Sandstone Member|39211|5|Briefly described|Fig.3|||See also Fig.4||||||
20695|Wyandra Sandstone Member|39478|6|Mentioned|Table 1|||||||||
20695|Wyandra Sandstone Member|39480|6|Mentioned|p196|||||||||
20695|Wyandra Sandstone Member|39481|6|Mentioned|p181|||||||||
20695|Wyandra Sandstone Member|39846|6|Mentioned|p48|||||||||
20695|Wyandra Sandstone Member|39847|5|Briefly described|p38|||||||||
20695|Wyandra Sandstone Member|39989|4|Described|p423|||||||||
20695|Wyandra Sandstone Member|40199|4|Described|p25|||||||||
20695|Wyandra Sandstone Member|40249|6|Mentioned|p41|||||||||
20695|Wyandra Sandstone Member|40681|6|Mentioned|Fig.2|||||||||
20695|Wyandra Sandstone Member|40687|3|Fully described|p417|||||||||
20695|Wyandra Sandstone Member|40832|6|Mentioned|p457|||||||||
20695|Wyandra Sandstone Member|40910|6|Mentioned|Table 3|||||||||
20695|Wyandra Sandstone Member|40926|6|Mentioned|Table 2|||||||||
20695|Wyandra Sandstone Member|41064|6|Mentioned|p62|||||||||
20695|Wyandra Sandstone Member|41089|6|Mentioned|p156|||||||||
20695|Wyandra Sandstone Member|41097|6|Mentioned|p165|||||||||
20695|Wyandra Sandstone Member|41165|5|Briefly described|p360|||||||||
20695|Wyandra Sandstone Member|41177|6|Mentioned|Fig.2|||||||||
20695|Wyandra Sandstone Member|41183|6|Mentioned|p310|||||||||
20695|Wyandra Sandstone Member|41186|5|Briefly described|p200|||||||||
20695|Wyandra Sandstone Member|41198|6|Mentioned|Table 1|||||||||
20695|Wyandra Sandstone Member|41219|6|Mentioned|p334|||||||||
20695|Wyandra Sandstone Member|41266|6|Mentioned|Fig.3|||||||||
20695|Wyandra Sandstone Member|41286|6|Mentioned|p117|||||||||
20695|Wyandra Sandstone Member|41523|5|Briefly described|p271|||||||||
20695|Wyandra Sandstone Member|41681|6|Mentioned|p23|||||||||
20695|Wyandra Sandstone Member|41724|6|Mentioned|p382|||||||||
20695|Wyandra Sandstone Member|42067|5|Briefly described|p313|||||||||
20695|Wyandra Sandstone Member|42084|6|Mentioned|Fig.3 P356|||||||||
20695|Wyandra Sandstone Member|42085|6|Mentioned|Fig.2 P374|||||||||
20695|Wyandra Sandstone Member|42999|5|Briefly described|Table 2,p90||Early Cretaceous|||||||
20695|Wyandra Sandstone Member|43105|5|Briefly described|Fig.9,p15.|||Of Cadna-owie Formation.||||||16-SEP-08
20695|Wyandra Sandstone Member|43122|5|Briefly described|p23|||of Cadna-owie Formation||||||
20695|Wyandra Sandstone Member|43602|5|Briefly described|203|||In Cadna-owie Formation||||||
20695|Wyandra Sandstone Member|44133|6|Mentioned|p115|||||||||
20695|Wyandra Sandstone Member|46791|6|Mentioned|Table 1|||See also Fig.7||||||
20695|Wyandra Sandstone Member|46937|5|Briefly described|Fig.10|||See also Table 1.||||||
20695|Wyandra Sandstone Member|46939|6|Mentioned|Fig.2|||||||||
20695|Wyandra Sandstone Member|49010|6|Mentioned|Fig.4|||Eromanga Basin||||||
20695|Wyandra Sandstone Member|49011|6|Mentioned|Fig.3|||Eromanga Basin||||||
20695|Wyandra Sandstone Member|60717|5|Briefly described|p40 Fig. 2|Early Cretaceous|Early Cretaceous|Of the Cadna-owie Formation. Overlain by Wallumbilla Formation and partly by Bulldog Shale. Geological Province: Eromanga Basin.||||||16-SEP-08
20695|Wyandra Sandstone Member|61014|5|Briefly described|pp532-554. |Lower Cretaceous|Lower Cretaceous|Eromanga Basin. The uppermost oil reservoir in the Eromanga Basin succession in south-west Queensland. Trace fossils (burrows) occur throughout. A regressive-transgressive sequence of fluvial, overbank crevasse-splay, mouth bar, estuarine and distal distributary channel deposits. Grain-size analysis and sequence-stratigraphic analogues are detailed.||Unit in Cadna-owie Formation.|||An amalgamation of fining-upward sandstone units to 2 m thick, with ripple cross-lamination, flaser bedding and multiple layers of carbonaceous detritus; commonly capped by thin mudstone units; interbedded mudstone and thin coal; bioturbated at top.|
20695|Wyandra Sandstone Member|61312|5|Briefly described|p64|Early Cretaceous|Early Cretaceous|Uppermost part of the Cadna-owie Formation. Dominantly sandstone; may contain reservoir quality sands. Geological Province: Eromanga Basin.||||||
20695|Wyandra Sandstone Member|61613|6|Mentioned|p282 Fig. 2|Early Cretaceous|Early Cretaceous|Of Cadna-owie Formation. Geological Province: Eromanga Basin.||||||07-FEB-11
20695|Wyandra Sandstone Member|61615|6|Mentioned|p302 Fig. 2|Early Cretaceous|Early Cretaceous|Geological Province: Eromanga Basin.||||||07-FEB-11
20695|Wyandra Sandstone Member|62029|5|Briefly described|p15 Fig. 4|Cretaceous|Cretaceous|||||||
20695|Wyandra Sandstone Member|62730|5|Briefly described|p352 Fig. 1|Early Cretaceous|Early Cretaceous|Of the Cada-owie Formation. Geological Province: Eromanga Basin.||||||21-APR-08
20695|Wyandra Sandstone Member|63979|5|Briefly described|p46, Fig. 44|Barremian|Hauterivian|Of (upper) Cadna-owie Formation occupying same stratigraphic position in Qld. as Mount Anna Sandstone in SA. A major aquifer in Great Artesian Basin. Geological province: Eromanga Basin.||||||07-FEB-11
20695|Wyandra Sandstone Member|64048|5|Briefly described|p71, p72|||Of the Cadna-owie Formation. Records high oil flow rates.||||||07-FEB-11
20695|Wyandra Sandstone Member|64197|6|Mentioned|p625 Fig.1c|Cretaceous|Cretaceous|Eromanga Basin.||Unit in Cadna-owie Formation.||Is overlain by Bulldog Shale or Wallumbilla Formation.||
20695|Wyandra Sandstone Member|65385|5|Briefly described|pS134 Fig.7|Early Cretaceous|Early Cretaceous|Of Cadna-owie Formation. Overlain by Wallumbilla Formation and Bulldog Shale.||||||08-MAR-12
20695|Wyandra Sandstone Member|66529|6|Mentioned|p12 Fig.5|||||Unit in Cadna-owie Formation.||||
20695|Wyandra Sandstone Member|66623|3|Fully described|p239, p243, pp254-255.|Early Cretaceous|Early Cretaceous|Equivalent to the informal Mokely Creek Sandstone member (Morton 1982), and topmost Gum Vale Beds. Glacial dropstones preserved towards the top. A widespread marker unit in Tibooburra-Milparinka area. Thickness to 20 m. Similar fossil assemblage as Cadna-owie Formation. Upper boundary is strongly diachronous, younging towards basin margins.||Unit in Cadna-owie Formation.||Is conformably, but sharply overlain by Wallumbilla Formation (or, in SA, by Bulldog Shale).|Calcareous quartzose sandstone, pebbly sandstone and quartz pebble conglomerate; exotic lonestone cobbles and boulders of quartz-veined quartzite and felsic volcanic lithologies common throughout.|05-JUN-13
20695|Wyandra Sandstone Member|66915|4|Described|p6 Fig.3, p9, p11 Fig.7|Early Cretaceous|Early Cretaceous|Eromanga Basin. Abbreviated as Wyandra Sandstone in some figures and text. See also parent Cadna-owie in this paper.||Uppermost unit of Cadna-owie Formation.||Is overlain by Wallumbilla Formation.||12-JAN-17
20695|Wyandra Sandstone Member|66921|5|Briefly described|Map legend|Cretaceous|Cretaceous|||Unit in Cadna-owie Formation.|||Coarse, calcareous, quartzose sandstone, pebbly sandstone and conglomerate.|
20695|Wyandra Sandstone Member|67207|5|Briefly described|Map legend.|Cretaceous|Cretaceous|||Unit in Cadna-owie Formation.|||Coarse, calcareous, quartzose sandstone, pebbly sandstone and conglomerate; local ferruginous, coarse, calcareous, quartzose sandstone, pebbly sandstone and conglomerate.|
20695|Wyandra Sandstone Member|67209|5|Briefly described|Map legend.|Cretaceous|Cretaceous|||Unit in Cadna-owie Formation.||Overlies Namur Sandstone.|Coarse, calcareous, quartzose sandstone, pebbly sandstone and conglomerate.|
20695|Wyandra Sandstone Member|67211|5|Briefly described|Map legend.|Cretaceous|Cretaceous|||Unit in Cadna-owie Formation.|||Coarse, calcareous, quartzose sandstone, pebbly sandstone and conglomerate.|
20695|Wyandra Sandstone Member|67323|5|Briefly described|p87|Early Cretaceous|Early Cretaceous|Eromanga Basin.||Cadna-owie Formation.||Is overlain by Wallumbilla Formation.||
20695|Wyandra Sandstone Member|67402|4|Described|p26, p26 tbl RRM4|Aptian|Aptian|Eromanga Basin. Maximum thickness of <10m. Deposited as beach sands during a marine transgressive cycle. Minor hydrocarbon reservoir but may be a major carbon dioxide storage reservoir. See also p43 tbl HPB1, p108, p109, p115, p121, p303.||Cadna-owie Formation.||Overlies the Lower Cadna-owie Formation. Overlain by the Wallumbilla Formation.|Mainly fine to medium-grained, thickly bedded sandstone with minor siltstone at the top.|
20695|Wyandra Sandstone Member|67561|5|Briefly described|p51, p52 Fig.2, p53, p64, p65, p67|Barremian|Valanginian|Eromanga Basin. Australian Spore-Pollen zonation: C.wonthaggiensis. Occurs at the top of the Cadna-Owie Formation. Previously regarded as a lowstand section, but re-interpreted by Bron (2010) as a tsunami deposit generated by the (125 +/- 1 Ma) Tookoonooka impact.||Of the Cadna-Owie Formation.||Overlain by the Bulldog Shale.|Coarse-grained sandstone.|20-JAN-17
20695|Wyandra Sandstone Member|68731|6|Mentioned|pp209-211|||||||||
20695|Wyandra Sandstone Member|69457|5|Briefly described|p41:3, 7|Early Cretaceous|Early Cretaceous|Senior et al. (1975). Eromanga Basin. Transitional (?beach setting) deposits.||Cadna-owie Formation.||Stratigraphic equivalent to Wyandra Sandstone Member (in Qld).||12-JUL-16
20695|Wyandra Sandstone Member|69594|5|Briefly described|p519, p526-528|Aptian|Barremian|Eromanga Basin. 3-18m thick. An important regional aquifer. A prominent regional marker. Beach deposits.||Topmost Cadna-owie Formation.||Is overlain by Doncaster Member (Wallumbilla Formation)..|Coarse, sporadically pebbly, quartzose to sublabile sandstone.|
20695|Wyandra Sandstone Member|69673|6|Mentioned|p155 fig 127|Cretaceous|Cretaceous|||Cadna-owie Formation||Overlain by Doncaster Member||
20695|Wyandra Sandstone Member|69797|5|Briefly described|p17 Fig.2|Early Cretaceous|Early Cretaceous|Geol. Prov: Eromanga Basin. Presented in figure as Wyandra Sandstone Mbr.||Cadna-owie Formation||||
20695|Wyandra Sandstone Member|69946|3|Fully described|p19-21, p57, p94|Early Cretaceous|Early Cretaceous|Eromanga Basin. Defined in the subsurface in Qld (Senior et al., 1975) as the upper sandy part of the Cadna-owie Formation. Type section is the interval 357 - 373m in Water Bore No. 2049 (Queensland Irrigation and Water Supply records), 15km SE of Wyandra. Proposal for a new type section discussed. Can be correlated on wireline logs into the Cooper region in SA. 3-18m thick in Qld (subsurface). Wireline log correlations.||Uppermost unit in Cadna-owie Formation.||Is overlain conformably by Bulldog Shale or Wallumbilla Formation.|Medium- to coarse-grained, quartzose to labile sandstone with scattered pebbles. Locally contains up to 40% feldspar and rock fragments.|
20695|Wyandra Sandstone Member|69947|5|Briefly described|p9, p13 Fig.7.2, p31-32 Figs.7.20-21|Early Cretaceous|Early Cretaceous|Lang et al. (2001). Eromanga Basin. Basal regional sequence boundary, overlain by amalgamated fluvial distributary channel fill. Appears simply as Wyandra Sandstone in Fig.7.20. Generalised stratigraphic log showing key surfaces and systems tracts.||Cadna-owie Formation||Is overlain by Bulldog Shale and the Wallumbilla Formation.|Basal in-filled fluvial channel sediments overlain by tidally-influenced sediments followed by heterolithic marine strata.|07-FEB-18
20695|Wyandra Sandstone Member|70649|5|Briefly described|Map Legend|Cretaceous|Cretaceous|||Cadna-owie Formation|||Coarse, calcareous, quartzose sandstone, pebbly sandstone and conglomerate.|
20695|Wyandra Sandstone Member|70652|5|Briefly described|Map Legend|Cretaceous|Cretaceous|||Cadna-owie Formation|||Coarse-grained, calcareous, quartzose sandstone, pebbly sandstone and conglomerate.|
20695|Wyandra Sandstone Member|70821|4|Described|p21 Fig.2.6, p22, p33, p79-80,p82,p85-86|Early Cretaceous|Early Cretaceous|Eromanga Basin. Typically 3-18m thick; locally considerably thicker. Historically considered a beach deposit; more recent work suggests it may well be an impact tsunami deposit formed by the Tookoonooka impact event to the NE of the project area (Bron, 2009). Hydrochemistry mentioned, hydrostratigraphic properties. Aquifer: generally artesian.||Cadna-owie Formation.||Is overlain by Doncaster Member (Wallumbilla Formation).|Coarse, sporadically pebbly, quartzose to sub-labile sandstone. Locally with dark carbonaceous laminae.|
20695|Wyandra Sandstone Member|71251|4|Described|p8, p11, p13, p15, p17, p19-20, p29|||See also p48-49, p51. Eromanga Basin. 30m total thickness in Eulo 1 borehole. An aquifer. Natural gamma, magnetic susceptibility data tabulated. Abbreviated in text to Wyandra Sandstone or simply Wyandra. Conductivity diagram.||Cadna-owie Formation.||Is overlain by Wallumbilla Formation.|Fine- to medium-grained sandstone, subangular quartz, feldspar and lithic fragments.|
20695|Wyandra Sandstone Member|71342|4|Described|Ch5 p19-p21, Ch5 p57, Ch6 p7|Aptian|Barremian|This unit was first defined by Senior et al (1975) as the upper sandy part of the Cadna-owie Formation. An initial type section was nominated by Senior et al (1975) however, Green, Brain et al (1989) proposed that a new type section was necessary if the original concept of Senior et al was to continue. This unit ranges between 3 and 18m thick in Queensland. Spore-pollen zone is given in Ch5 p57. Hosts commercially producible oil in Aldinga 1. Seal and reservoir characteristics discussed in Ch11. See also  Ch7 p9, Ch7 p11, Ch7 p13, Ch7 p32, Ch11 p2, Ch11 p5, Ch12 p3.||Cadna-owie Formation||Conformably overlain by the Wallumbilla Formation or the Bulldog Shale.|Medium to coarse-grained, quartzose to labile sandstone with scattered pebbles. Sandstones may contain up to 40% feldspar and rock fragments.|
20695|Wyandra Sandstone Member|71863|6|Mentioned|p5|Aptian|Aptian|Eromanga Basin.||Cadna-owie Formation||Overlain by the Doncaster Member.||
20695|Wyandra Sandstone Member|71864|6|Mentioned|p13-p14, p17, p26|||Waterbores are reported to intersect this unit which is a moderately producing aquifer.||Cadna-owie Formation||||
20695|Wyandra Sandstone Member|72297|5|Briefly described|p743|||Eromanga Basin. High oil flows recorded at Talgeberry.||||||
20695|Wyandra Sandstone Member|72298|5|Briefly described|p801|Cretaceous|Cretaceous|Eromanga Basin (QLD,NSW). Main confined aquifers, generally producing flowing artesian water bores.||Cadna-owie FZ.||Is overlain by Doncaster Member (Wallumbilla FZ).||
20695|Wyandra Sandstone Member|72914|5|Briefly described|p14-16, p18, p20-21, p27, p29-30, App.I|Cretaceous|Cretaceous|Major groundwater source in the local region; supplies fresh to slightly brackish water. Natural gamma emissions are very subdued, indicating the quartz-rich nature of the unit. See also accidental misspelling Wyandra Sandstone member p20.||Cadna-owie Formation||Overlain by the Wallumbilla Formation.|Clean quartz sandstone; quartzose and labile lithic gravels.|
20695|Wyandra Sandstone Member|72915|6|Mentioned|p27|Mesozoic|Mesozoic|Constitutes a local aquifer.||Cadna-owie Formation||||
20695|Wyandra Sandstone Member|73167|6|Mentioned|p664 Fig. 2|Cretaceous|Cretaceous|Eromanga Basin. Contains oil and gas.||Cadna-owie Formation||||
20695|Wyandra Sandstone Member|73251|6|Mentioned|p62|Early Cretaceous|Early Cretaceous|||Cadna-owie Formation||Overlain by Wallumbilla Formation.||
20695|Wyandra Sandstone Member|73343|6|Mentioned|p337|Cretaceous|Cretaceous|Eromanga Basin.||Cadna-owie Formation||Overlain by Wallumbilla Formation.||
20695|Wyandra Sandstone Member|73479|5|Briefly described|p156 Fig.2, p159|Cretaceous|Cretaceous|Eromanga Basin. Deltaic shoreface marine depositional environment.|ca 125 Ma|Cadna-owie Formation||Overlies Cadna-owie Formation||
20730|Wywyana Formation|22772|5|Briefly described|Table13.1|Cryogenian|Cryogenian|||||||
20730|Wywyana Formation|22857|5|Briefly described|Tb. 13.1 (insert p70-71)|Willouran|Willouran|Of the Arkaroola Subgroup (Callanna Group).||||||
20730|Wywyana Formation|22926|6|Mentioned|42|||||||||
20730|Wywyana Formation|23394|5|Briefly described|Map legend|Proterozoic|Proterozoic|||||||
20730|Wywyana Formation|23411|6|Mentioned|Map Legend|||||||||
20730|Wywyana Formation|23412|5|Briefly described|Map Legend|Proterozoic|Proterozoic|||||||
20730|Wywyana Formation|23562|5|Briefly described|p295 Fig 2|Cryogenian|Cryogenian|||||||
20730|Wywyana Formation|23818|6|Mentioned|p53|||Max. thickness: 360 ft.||||||
20730|Wywyana Formation|24175|6|Mentioned|p8|||Geological province: Mount Painter province.||||||
20730|Wywyana Formation|24176|4|Described|p9, p26 Tb. 1|Adelaidean|Adelaidean|Of the Callanna Beds. Dolomitic and actinolitic marbles.  Age is Willouran. Overlies and intertongues with Paralana Quartzite. Max. thickness: 460m. Geological Province: Mount Painter Province.||||||13-FEB-08
20730|Wywyana Formation|24546|5|Briefly described|p2 - 3 Fig.2|Neoproterozoic|Neoproterozoic|Overlies Paralana Quartzite. Overlain by Wooltana Volcanics. Of Arkaroola Subgroup. Geological Province: Adelaide Fold Belt.||||||16-JAN-08
20730|Wywyana Formation|24586|5|Briefly described|p53|Adelaidean|Adelaidean|Of the Callana Group (Warrina Supergroup).||||||
20730|Wywyana Formation|24593|5|Briefly described|p612 Fig. 1a|Adelaidean|Adelaidean|Of the Callana Group.  Geological Province: Mount Painter Inlier.  See also p613 Fig. 1b.||||||
20730|Wywyana Formation|29840|6|Mentioned|Fig.3|||||||||
20730|Wywyana Formation|30028|6|Mentioned|p370|||||||||
20730|Wywyana Formation|30176|6|Mentioned|Map legend|Adelaidean|Adelaidean|Willouran||||||
20730|Wywyana Formation|30177|2|Defined|p127|Adelaidean|Adelaidean|See also p52. Type section: Arkaroola Creek, 3.4 miles north of Arkaroola Homestead, lat. 30degrees 17'01"S  long. 139degrees22'35"E to lat. 30degrees17'08"S  long. 139degrees22'30"E.||||||08-DEC-22
20730|Wywyana Formation|30261|6|Mentioned|Table 1|||Willouran age||||||
20730|Wywyana Formation|30712|5|Briefly described|p56|||||||||
20730|Wywyana Formation|30801|6|Mentioned|p5|||Lower Callanna Beds. Table P5-6.||||||
20730|Wywyana Formation|30807|6|Mentioned|p103|||Suggested map symbol||||||
20730|Wywyana Formation|30917|6|Mentioned|p38|||||||||
20730|Wywyana Formation|31541|6|Mentioned|p544|||||||||
20730|Wywyana Formation|32724|6|Mentioned|Fig.1|||Correlation. Willouran||||||
20730|Wywyana Formation|32823|6|Mentioned|p361|||||||||
20730|Wywyana Formation|33474|6|Mentioned|Fig.4|||||||||
20730|Wywyana Formation|34176|6|Mentioned|p51|||||||||
20730|Wywyana Formation|34269|6|Mentioned|Table 1|||||||||
20730|Wywyana Formation|34535|4|Described|p53|||||||||
20730|Wywyana Formation|34812|6|Mentioned|p134|||See also Table 8.||||||
20730|Wywyana Formation|34957|6|Mentioned|p395|||||||||
20730|Wywyana Formation|35255|6|Mentioned|p13|||||||||
20730|Wywyana Formation|35692|6|Mentioned|p23|||||||||
20730|Wywyana Formation|36245|6|Mentioned|p9|||||||||
20730|Wywyana Formation|36514|6|Mentioned|p59|||||||||
20730|Wywyana Formation|36731|6|Mentioned|p122|||Fig.3||||||
20730|Wywyana Formation|36733|6|Mentioned|p56|||||||||
20730|Wywyana Formation|37461|4|Described|p335|||See also Table 5.I||||||
20730|Wywyana Formation|37854|6|Mentioned|p8|||||||||
20730|Wywyana Formation|38157|6|Mentioned|Table II|||||||||
20730|Wywyana Formation|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Willouran||||||
20730|Wywyana Formation|39348|6|Mentioned|Map legend|Adelaidean|Adelaidean|Willouran||||||
20730|Wywyana Formation|39490|6|Mentioned|p10|||||||||
20730|Wywyana Formation|40294|6|Mentioned|p8|||See also P52||||||
20730|Wywyana Formation|41403|3|Fully described|p49|||||||||
20730|Wywyana Formation|42098|5|Briefly described|Table 2 P54|||||||||
20730|Wywyana Formation|42222|5|Briefly described|p11|||||||||
20730|Wywyana Formation|42223|6|Mentioned|p46|||||||||
20730|Wywyana Formation|42238|6|Mentioned|p71|||||||||
20730|Wywyana Formation|42760|6|Mentioned|p3|||||||||
20730|Wywyana Formation|43052|5|Briefly described|p172|||Of Arkaroola Subgroup.||||||13-FEB-08
20730|Wywyana Formation|43742|6|Mentioned|p42|||||||||
20730|Wywyana Formation|43845|6|Mentioned|p43||Neoproterozoic|In Arkaroola Subgroup. Willouran age.||||||12-JUL-16
20730|Wywyana Formation|44133|6|Mentioned|p54|||||||||
20730|Wywyana Formation|60718|6|Mentioned|p49|Adelaidean|Adelaidean|Possible evaporite unit.||Of Arkaroola Subgroup, Mount Painter Inlier.||Overlies Paralana Quartzite; underlies Wooltana Volcanics.||15-APR-11
20730|Wywyana Formation|61239|6|Mentioned|p56|||In the Mount Painter region.||||||
20730|Wywyana Formation|61523|5|Briefly described|p12|Adelaidean|Adelaidean|Geolgocial Province: Mount Painter Province.||||||
20730|Wywyana Formation|62592|5|Briefly described|p50 Table 5.1, p57.|Willouran|Willouran|Adelaide Geosyncline.||Unit in Arkaroola Subgroup.||Overlies Paralana Quartzite gradationally. Is overlain by Wooltana Volcanics.|Limestone, dolomite, calc-silicate.|
20730|Wywyana Formation|62993|5|Briefly described|p30|Neoproterozoic|Neoproterozoic|||Arkaroola Subgroup|||Calc-silicate rocks.|
20730|Wywyana Formation|65925|5|Briefly described|p124 Fig.3, p136, Appendix 2.|Neoproterozoic|Neoproterozoic|Near Lady Buxton Copper Mine, this unit has been thrust over Cenozoic sediments.||Unit in Arkaroola Subgroup.|||Calcsilicate; marble; actinolite amphibolite; passes laterally to diapiric habit.|
20730|Wywyana Formation|67870|5|Briefly described|p9|Neoproterozoic|Neoproterozoic|Adelaide Rift System.||Arkaroola Subgroup.||||
20730|Wywyana Formation|69019|6|Mentioned|p36.|Neoproterozoic|Neoproterozoic|||||||
20730|Wywyana Formation|70384|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Adelaide Geosyncline. Age shown more specifically as Willouran [basal Cryogenian].||Arkaroola Subgroup.||Conformably overlies Paralana Quartzite. Is overlain by Wooltana Volcanics.|Calcsilicate; marble; actinolite amphibolite.|18-JAN-19
20730|Wywyana Formation|73222|6|Mentioned|p7|Tonian|Tonian|Adelaide Rift Complex, Gammon Ranges. Willouran.||Arkaroola Subgroup, Callanna Group, Warrina Supergroup||Underlain by Paralana Quartzite. Overlain[?] by Wooltana Volcanics. Possibly equivalent to Black Knob Marble.||
20730|Wywyana Formation|74367|6|Mentioned|p7 Fig.6|||||Arkaroola Subgroup||||
20745|Yagdlin Phyllite|23394|5|Briefly described|Map legend|Proterozoic|Proterozoic|||||||
20745|Yagdlin Phyllite|23411|6|Mentioned|Map Legend|||||||||
20745|Yagdlin Phyllite|30177|2|Defined|p123|Paleoproterozoic|Paleoproterozoic|See also p32. Type section Three quarters of a mile east-southeast to two miles southwest of Mount Adams, lat. 30degrees06'23"S, long. 139degrees31'28"E to lat. 30degrees06'49"S, long. 139degrees 32'34"E.||||||24-NOV-22
20745|Yagdlin Phyllite|30807|6|Mentioned|p103|||Suggested map symbol||||||
20745|Yagdlin Phyllite|30920|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Prob.Lower Proterozoic||||||07-NOV-08
20745|Yagdlin Phyllite|42624|5|Briefly described|p30|||||||||
20745|Yagdlin Phyllite|43052|5|Briefly described|p149|||||||||
20745|Yagdlin Phyllite|60953|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Sandy and silty phyllite.||||||
20745|Yagdlin Phyllite|61108|5|Briefly described|map legend|Mesoproterozoic|Mesoproterozoic|Sandy and silty phyllite.||||||
20745|Yagdlin Phyllite|62962|6|Mentioned|p2284 Fig. 2|Mesoproterozoic|Mesoproterozoic|Geological Province: Mount Painter Province.||||||07-FEB-11
20745|Yagdlin Phyllite|63489|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Included in undifferentiated pelitic metasediments. Geological Province: Mount Painter Inlier.||||||10-SEP-07
20745|Yagdlin Phyllite|66302|6|Mentioned|p39, p49|||Moolawatana Domain, Curnamona Province.|1595 to 1591 Ma|||||
20745|Yagdlin Phyllite|67323|6|Mentioned|Eastern Australia Time-Space Plot|||Mount Painter area.||||||
20745|Yagdlin Phyllite|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.|
20745|Yagdlin Phyllite|67540|6|Mentioned|p33 Tb.2|||||Unit in Radium Creek Metamorphics.||Faulted against/intruded by Coulthard Suite.||04-FEB-16
20745|Yagdlin Phyllite|67653|6|Mentioned|p4|||Geological province: Curnamona Province.||||||
20745|Yagdlin Phyllite|69023|6|Mentioned|p52|||Coats and Blissett (1971).|~1585-~1570 Ma.|||||
20745|Yagdlin Phyllite|69650|6|Mentioned|p8, p62, p64|||||Unit in Radium Creek Metamorphics.||Is intruded by Coulthard Suite.||
20745|Yagdlin Phyllite|69654|6|Mentioned|p3|||Curnamona Province.||||||
20745|Yagdlin Phyllite|70384|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Phyllite hornfelsed by intrusion of Mount Neill Granite.||Radium Creek Group.|||Phyllite, schist. East of Paralana Fault Zone. A separately mapped sub-unit contains phyllite, hornfelsed due to intrusion of Mount Neill Granite.|16-JAN-19
20776|Yallunda Ferricrete|23818|5|Briefly described|p226 Fig.121|Early Pleistocene|Early Pleistocene|||||||
20776|Yallunda Ferricrete|32438|6|Mentioned|p42|||||||||
20776|Yallunda Ferricrete|34180|6|Mentioned|p226|||Tertiary.||||||
20787|Yamba Formation|22531|6|Mentioned|p6|||||||||
20787|Yamba Formation|22773|5|Briefly described|p339|Holocene|Late Pleistocene|||||||
20787|Yamba Formation|22782|4|Described|p17|||||||||
20787|Yamba Formation|22799|3|Fully described|p55|Holocene|Late Pleistocene|||||||
20787|Yamba Formation|22857|5|Briefly described|p339|Holocene|Late Pleistocene|Lacustrine and lunette sediments with gypsum deposits. Geological Province: Murray Basin.||||||
20787|Yamba Formation|23818|5|Briefly described|p212 Fig.108|Recent|Recent|Geological Province: Great Artesian Basin and Murray Basin.||||||
20787|Yamba Formation|23908|6|Mentioned|p6|||Overlies Gawler Craton rocks.||||||04-NOV-10
20787|Yamba Formation|23921|5|Briefly described|p1109 Table 1|Quaternary|Quaternary|Geological Province: Murray Basin.||||||
20787|Yamba Formation|24358|5|Briefly described|p32 Fig.1|||||||||04-NOV-10
20787|Yamba Formation|24551|5|Briefly described|p388 Fig. 11.2, 340|Holocene|Middle Pleistocene|Overlies Blanchetown Clay.||||||02-JUL-13
20787|Yamba Formation|24574|6|Mentioned|p706|||||||||
20787|Yamba Formation|30581|6|Mentioned|Map legend|Quaternary|Quaternary|||||||
20787|Yamba Formation|30751|6|Mentioned|Map legend|Recent|Recent|||||||
20787|Yamba Formation|30753|4|Described|p15|||Recent age||||||
20787|Yamba Formation|30754|2|Defined|Appendix 1|Recent|Recent|||||||
20787|Yamba Formation|30755|6|Mentioned|p169|||Tectonic map||||||
20787|Yamba Formation|30756|6|Mentioned|p2|||||||||
20787|Yamba Formation|30807|6|Mentioned|p101|||Suggested map symbol||||||
20787|Yamba Formation|30922|6|Mentioned|Map legend|Holocene|Holocene|||||||
20787|Yamba Formation|30934|6|Mentioned|Map legend|Recent|Recent|||||||
20787|Yamba Formation|30935|6|Mentioned|Map legend|Recent|Recent|||||||
20787|Yamba Formation|31312|6|Mentioned|p70|||||||||
20787|Yamba Formation|31320|6|Mentioned|Fig.1|||Quaternary||||||
20787|Yamba Formation|31741|6|Mentioned|p6|||||||||
20787|Yamba Formation|31745|6|Mentioned|Map legend|Recent|Recent|||||||
20787|Yamba Formation|31747|6|Mentioned|Map legend|Quaternary|Quaternary|||||||
20787|Yamba Formation|31850|4|Described|p40|||||||||
20787|Yamba Formation|32426|6|Mentioned|p142|||Stratigraphic table. Renmark area.||||||
20787|Yamba Formation|32435|6|Mentioned|Fig.1|||||||||
20787|Yamba Formation|32437|6|Mentioned|Fig.2|||||||||
20787|Yamba Formation|32438|6|Mentioned|Fig.2|||||||||
20787|Yamba Formation|34180|6|Mentioned|p212|||Recent||||||
20787|Yamba Formation|34536|6|Mentioned|Map legend|Recent|Recent|Equivalent||||||
20787|Yamba Formation|34965|6|Mentioned|p417|||||||||
20787|Yamba Formation|35029|6|Mentioned|p166|||||||||
20787|Yamba Formation|35097|6|Mentioned|Fig.4|||||||||
20787|Yamba Formation|35200|6|Mentioned|Map legend|Holocene|Holocene|||||||
20787|Yamba Formation|35232|5|Briefly described|Table.4|||||||||
20787|Yamba Formation|35272|5|Briefly described|p284|||||||||
20787|Yamba Formation|35772|6|Mentioned|p13|||||||||
20787|Yamba Formation|37873|5|Briefly described|p4|||||||||
20787|Yamba Formation|38068|5|Briefly described|p79|||||||||
20787|Yamba Formation|40215|6|Mentioned|p56|||||||||
20787|Yamba Formation|40448|6|Mentioned|p43|||||||||
20787|Yamba Formation|40941|6|Mentioned|Map legend|Holocene|Holocene|||||||
20787|Yamba Formation|40942|4|Described|p23|||||||||
20787|Yamba Formation|41499|6|Mentioned|p70|||||||||
20787|Yamba Formation|41848|5|Briefly described|p359|Recent|late Quaternary|Overlies Blanchetown Clay||||||
20787|Yamba Formation|41868|6|Mentioned|p571|||||||||
20787|Yamba Formation|42125|6|Mentioned|p139|||||||||
20787|Yamba Formation|42126|6|Mentioned|Fig.8 P155|||||||||
20787|Yamba Formation|42134|4|Described|p339|||||||||
20787|Yamba Formation|42136|4|Described|Table 1 P364|||||||||
20787|Yamba Formation|42292|6|Mentioned|Fig.1 P9|||||||||
20787|Yamba Formation|42466|6|Mentioned|Map Legend|||||||||
20787|Yamba Formation|42475|6|Mentioned|p26|||||||||
20787|Yamba Formation|42716|5|Briefly described|Map legend|Holocene||||||||
20787|Yamba Formation|42717|5|Briefly described|map legend|Holocene||||||||
20787|Yamba Formation|42738|5|Briefly described|map legend|Quaternary||||||||
20787|Yamba Formation|42827|5|Briefly described|p359|||see also Table 9.1||||||
20787|Yamba Formation|42881|6|Mentioned|Fig.2, P83|||||||||
20787|Yamba Formation|42966|1|Redefined|p252|Holocene|Late Pleistocene|||||||
20787|Yamba Formation|43049|5|Briefly described|p27|||||||||
20787|Yamba Formation|43053|5|Briefly described|Map Legend|Holocene|Holocene|||||||25-MAY-05
20787|Yamba Formation|43073|5|Briefly described|Table 4|||||||||
20787|Yamba Formation|43258|5|Briefly described|Map Legend||Holocene|||||||
20787|Yamba Formation|43298|5|Briefly described|Map Legend||Holocene|||||||
20787|Yamba Formation|43655|5|Briefly described|p40-846|||||||||
20787|Yamba Formation|43669|4|Described|p23-24|||||||||
20787|Yamba Formation|44133|5|Briefly described|p252|Holocene|Middle Pleistocene|Parts equivalent to Tyrrell Beds. Geological Province: Murray Basin.||||||
20787|Yamba Formation|44191|5|Briefly described|Map Legend||Late Pleistocene|||||||
20787|Yamba Formation|44660|14|Not recorded|map legend|||Recent, lithology.||||||
20787|Yamba Formation|44864|6|Mentioned|Map Legend||Holocene|||||||
20787|Yamba Formation|49038|5|Briefly described|p32|||||||||
20787|Yamba Formation|60005|5|Briefly described|Map legend|Holocene|Pleistocene|Aeolianites and evaporites: fine-grained gypsum.||||||11-JAN-10
20787|Yamba Formation|60953|5|Briefly described|Map Legend|Holocene|Pleistocene|||||||
20787|Yamba Formation|61070|6|Mentioned|Map Legend|Quaternary|Quaternary|||||||12-JAN-10
20787|Yamba Formation|61108|5|Briefly described|map legend|Quaternary|Quaternary|Lacustrine gypsiferous, saline and organic clay, silt and sand of modern playas and lakes.||||||
20787|Yamba Formation|62893|4|Described|Map Legend, p24-25|Holocene|Holocene|Lacustrine and aeolian; represents inland lakes occupying depressions in the Bridgewater Formation.|||||Halite, gypsite, gypsarenite, selenite and minor carbonate and gypsiferous mud.|
20787|Yamba Formation|65552|6|Mentioned|p23 App.2|Quaternary|Quaternary|Murray Basin unit. Hosts gypsum resources.||||||
20787|Yamba Formation|65715|5|Briefly described|p15 Tb.8, p25|Neogene|Neogene|Defined by Firman (1966).||||||
20787|Yamba Formation|66002|5|Briefly described|p13 Tb.9|Neogene|Neogene|Defined by Firman 1966.||||||
20787|Yamba Formation|67179|4|Described|p581, p582|Holocene|Pleistocene|Late Pleistocene to Holocene, deposited on the beds of saline lakes. Up to 1.5 m thick in Lake Tuchewop.|||||Friable gypsiferous clay, pelletal clay, gypsum-quartz sand aggregates and gypsum (Brown and Stevenson 1991), halite.|
20787|Yamba Formation|68116|5|Briefly described|Appendix, Maps 1-11, 14-16, 21, 22, 29.|Holocene|Pleistocene|Late Pleistocene maximum age.  Lacustrine evaporite deposits.|||||Pale grey gypsite, gypsiferous clay and grey pelletal gypsum-quartz sand aggregates; locally includes grey clay with crystalline gypsum mush under black sulphide-rich mud with ephemeral crusts of gypsum, halite, bischofite, thenardite and mirabilite.|
20787|Yamba Formation|68131|5|Briefly described|p71, p84|Holocene|Pleistocene|Flinders Island, Nuyts Domain, Gawler Craton.||||||
20787|Yamba Formation|70334|5|Briefly described|p74|||Modern saline playa deposits, occurring behind the Saint Kilda Formation at the head of False Bay.|||||Gypsiferous clay and gypsum-quartz sand mixtures and gypsum associated with dunes of seed and flour gypsum.|
20787|Yamba Formation|70337|5|Briefly described|Map legend.|Holocene|Pleistocene||||||Clay, lacustrine, gypsiferous, gypsum-quartz sand. Dunes, playa lakes.|
20787|Yamba Formation|73188|6|Mentioned|p320|Pleistocene|Pleistocene|Murray Basin.|||||Alluvial fans, clay, sand, gravel, wind-blown sand.|
20787|Yamba Formation|73496|5|Briefly described|Map legend|Holocene|Holocene||||||Evaporitic and associated clay deposits in topographic lows; nonmagnetic; low to high K, Th, U depending on water content.|
20809|Yancowinna Subgroup|22772|4|Described|p66,Table13.1|Cryogenian|Cryogenian|||||||
20809|Yancowinna Subgroup|22857|5|Briefly described|p66, Tb. 13.1 (insert p70-71)|Sturtian|Sturtian|Of the Torrowangee Group. Age: ~700Ma. Max. thickness: 200m. See also p398 App. 1 Tb.A1.3.||||||
20809|Yancowinna Subgroup|36733|6|Mentioned|Table 5|||||||||
20809|Yancowinna Subgroup|37238|6|Mentioned|p355|||||||||
20809|Yancowinna Subgroup|38157|6|Mentioned|p261|||||||||
20809|Yancowinna Subgroup|40294|6|Mentioned|p48|||||||||
20809|Yancowinna Subgroup|41405|5|Briefly described|p203|||||||||
20809|Yancowinna Subgroup|42531|5|Briefly described|Map legend|Adelaidean||||||||
20809|Yancowinna Subgroup|43265|5|Briefly described|Map Legend||Neoproterozoic|Of the Torrowangee Group.||||||11-SEP-07
20809|Yancowinna Subgroup|62724|5|Briefly described|p17 Fig. 4|Sturtian|Sturtian|Of the Torrowangee Group. Geological Province: Broken Hill Domain.||||||07-FEB-11
20809|Yancowinna Subgroup|63489|5|Briefly described|Map legend|Adelaidean|Adelaidean|Diamictite, siltstone, sandstone, minor carbonate. South Australia equivalent is Yudnamutana Subgroup.||||||10-SEP-07
20809|Yancowinna Subgroup|68277|6|Mentioned|p96|Neoproterozoic|Neoproterozoic|The rank is not given in the text.||||||
20809|Yancowinna Subgroup|70000|5|Briefly described|p34, p39|Neoproterozoic|Neoproterozoic|||Unit in Torrowangee Group.|Includes McDougalls Well Conglomerate; Mulcatcha, Yangalla and Waukeroo Formations.|Is overlain by Euriowie Subgroup.|Diamictite (tillite), conglomerate, quartz sandstone and well-bedded siltstone/sandstone successions with abundant glacial clasts.|
20809|Yancowinna Subgroup|70015|5|Briefly described|Map legend|Cryogenian|Cryogenian|Mineral deposits (if any) are shown.||Unit in Torrowangee Group.|Includes McDougalls Well Conglomerate; Mulcatcha, Yangalla and Waukeroo Formations.|Is overlain by Euriowie Subgroup.|Poorly sorted grit, sandstone, diamictite and siltstone, minor carbonate.|
20817|Yandoolka Rhyolite|29838|2|Defined|p13|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
20817|Yandoolka Rhyolite|30984|2|Defined|p11|Proterozoic|Proterozoic|||||||
20817|Yandoolka Rhyolite|41974|5|Briefly described|Table 1 P412|||||||||
20817|Yandoolka Rhyolite|42721|5|Briefly described|map legend|Carpentarian||||||||
20817|Yandoolka Rhyolite|43094|4|Described|p28|||||||||
20817|Yandoolka Rhyolite|67909|6|Mentioned|p127|Mesoproterozoic|Mesoproterozoic|||Glyde Hill Volcanic Complex.||||
20817|Yandoolka Rhyolite|72090|6|Mentioned|p12|||Gawler Craton.||||||
20825|Yankaninna Formation|9862|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Of the Umberatana Group. White fine dolomite marble with talc.||||||
20825|Yankaninna Formation|22510|5|Briefly described|table1p37,41|||Status revised.  Of the Upalinna Subgroup.  Age: Marinoan. Revised Status. No longer member of Tapley Hill Formation.||||||13-OCT-04
20825|Yankaninna Formation|23818|6|Mentioned|p241 Fig.133|Neoproterozoic|Neoproterozoic|||||||
20825|Yankaninna Formation|30177|6|Mentioned|p79|||||||||25-NOV-22
20825|Yankaninna Formation|34268|6|Mentioned|p241|||U.Prot.||||||
20825|Yankaninna Formation|34291|6|Mentioned|p12|||||||||
20825|Yankaninna Formation|34534|6|Mentioned|Fig.2.13|||||||||
20825|Yankaninna Formation|41364|6|Mentioned|Fig.1|||||||||
20825|Yankaninna Formation|41405|6|Mentioned|p166|||||||||
20825|Yankaninna Formation|41647|6|Mentioned|Fig.2|||||||||
20825|Yankaninna Formation|41770|6|Mentioned|Fig.1|||||||||
20825|Yankaninna Formation|60718|5|Briefly described|p49 Fig. 2, p53, 55|Adelaidean|Adelaidean|Geological Province: Adelaide Geosyncline. See also p51 Fig. 3.||Of Upalinna Subgroup (Umberatana Group).||Unconformably overlies Tapley Hill Formation.||15-APR-11
20825|Yankaninna Formation|64846|5|Briefly described|p197 Fig.2, p198 Fig.3, p199 |Cryogenian|Cryogenian|See also p200 Fig.5, p202 Tb.1, p206 Tb.2. Carbon isotope details.||Of the Upalinna Subgroup.|||Includes basinal megabreccia and slope limestone units.|
20825|Yankaninna Formation|65493|5|Briefly described|p907, 915, 920, 924 |Cryogenian|Cryogenian|Of Upalinna Subgroup. Onlaps the Balcanoona Formation. Deep water carbonate and siliciclastic sediments. Basinal megabreccia and overlying slope limestones. Includes Bouma sequences. Also mentioned in Figs 1,2,4,6,10-11,13-15,17.||||||08-JUL-13
20825|Yankaninna Formation|65925|5|Briefly described|Appendix 2.||||||||Siltstone, grey-green, thinly bedded, calcareous, with lenses of dolomite.|
20825|Yankaninna Formation|67180|4|Described|p600-602, p606, p610-612, Figs. 1,2,4,10|Cryogenian|Cryogenian|Marinoan. Characterised by two or three distinct limestone beds that interbed with calcareous siltstones and shales. Basal unconformity equivalent to the Weetootla Dolomite basal unconformity, suggested as the Sturtian-Marinoan boundary.  Preiss et al. (1998) place the Sturtian-Marinoan boundary at the lower (erosional) contact of this unit with the underlying Balcanoona Formation. Giant ooids (8mm) where it onlaps the Balcanoona Fm.||Unit in Upalinna Subgroup||Disconformably overlies the Tapley Hill Formation, conformably underlies Amberoona Formation, direct lateral equivalent to the Weetootla Dolomite Member.|Calcareous silts and grey micritic limestone; calcareous/dolomitic shale, allochthonous blocks (Oodnaminta Reef Cmplex), laminated micritic limestone beds within calcareous silts and shales, soft sediment deformation and slumps, giant ooids (8mm).|
20825|Yankaninna Formation|67979|4|Described|p532-534, p528-530, p540-541, p543-545|Marinoan||Base marks Sturtian-Marinoan Series boundary in Nthn Flinders. Previously regarded as correlative with Etina Formation of Central Ranges (Preiss et al. 1998). Herein, Willigan Member (formerly uppermost in Tapley Hill Formation) now considered a localised lower member of Yankaninna Formation. See also informal upper and lower Yankaninna Formation herein. See also p536, 538,  Figs.10 and 11.||Upalinna Subgroup|Willigan Member|Conformable/erosional over Tapley Hill Formation. Overlain by Amberoona Fm.|Calcareous shaley-siltstones with three distinct bands of finely-laminated, slump folded, steel-grey limestone consistently observed in basal portion; above this, calcareous siltstones containing coarser sandy interbeds.|22-SEP-14
20825|Yankaninna Formation|68068|5|Briefly described|Map legend|Marinoan|Marinoan|Adelaide Geosyncline.||Unit in Upalinna Subgroup.||Unconformably overlies Balcanoona Formation. Is conformably overlain by Amberoona Formation.|Thinly-bedded grey siltstone with buff-weathering grey dolomite as diachronous lenses up to 30 m thick; basal conglomerate includes clasts of underlying Balcanoona Formation.|
20825|Yankaninna Formation|69019|4|Described|p43, p49-50, p144.|Neoproterozoic|Neoproterozoic|Defined by Coats (1964) and Thomson et al. (1964); redefined as Yankaninna Siltstone Member (of Tapley Hill Formation) by Coats and Blissett (1971); reverted to Formation status after revisions by Preiss et al. (1998) as it disconformably overlies Balcanoona Formation. Its absence or thinning indicates a depositional hiatus. Early Marinoan.||||Overlies Bolla Bollana Tillite unconformably or disconformably. Is overlain by Amberoona Formation, conformably or unconformably.|Greenish to greyish, thinly bedded calcareous siltstone that weathers to a yellowish hue; lenses of fine-grained recrystallised dolomite to sandy dolomite.|
20825|Yankaninna Formation|69023|5|Briefly described|p66-67, p70-72, p146|Neoproterozoic|Neoproterozoic|Originally defined by Coats (1964) and Thomson (1964); redefined as Yankaninna Siltstone Member (of Tapley Hill Formation) by Coats and Blissett (1971). Reid and Sheard found that it disconformably overlies Balcanoona Formation and hence could not be part of the (underlying) Tapley Hill Formation; its exclusion was formalised by Preiss et al. (1998). Now (Sheard, 2009) reverts to its original Formation status.||||Overlies Balcanoona Formation unconformably, and Bolla Bollana Tillite unconformably or disconformably. Is overlain by Amberoona Formation.|Greenish to greyish, thinly-bedded calcareous siltstone, weathering to grey to yellowish; conspicuous lenses of grey, fine-grained, recrystallised dolomite to sandy dolomite.|
20825|Yankaninna Formation|70021|6|Mentioned|p97|Neoproterozoic|Neoproterozoic|Northern Flinders Ranges, Adelaide Geosyncline.||||||
20825|Yankaninna Formation|70384|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Adelaide Geosyncline. Age shown more specifically as Marinoan [Cryogenian].||of Upalinna Subgroup.||Unconformably overlies Balcanoona Formation (Nepouie Subgroup).|Grey to grey-green, thinly-bedded calcareous siltstone; the basal conglomerate bed contains Balcanoona Formation clasts. A buff-weathering grey dolomite marble forms diachronous lenses <30m thick.|23-JAN-19
20825|Yankaninna Formation|71237|2|Defined|p7, 10, 11, 19|||||||||
20825|Yankaninna Formation|72456|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Marree 1:250k map sheet.|||||Siltstone, grey-green, thinly bedded, calcareous with lenses of dolomite.|14-JUN-22
20825|Yankaninna Formation|72613|6|Mentioned|p2 fig 1, p3|Cryogenian|Cryogenian|Shown as earliest Marinoan age. Northern Flinders Ranges.||Umberatana Group||Shown as unconformably overlying Angepena Formation.||
20825|Yankaninna Formation|73086|6|Mentioned|p78, p91|||Adelaide Rift Complex.||||May correlate to Ringwood and Limbla members (Aralka Formation).||
20845|Yardea Dacite|22629|5|Briefly described|p158|Calymmian|Calymmian|Age: 1592+/-3Ma||||||
20845|Yardea Dacite|22873|5|Briefly described|p9, p11|||Parent is Gawler Range Volcanics, maximum thickness is 250m, underlying unit is Nonning Rhyodacite||||||16-APR-18
20845|Yardea Dacite|24217|5|Briefly described|p833|Proterozoic|Proterozoic|Of the Gawler Range Volcanics.  Geological Province: Gawler Craton||||||
20845|Yardea Dacite|24346|3|Fully described|p102, 105|||Originally referred to as Gawler Range porphyry.  Defined as Yardea Dacite Formation in Appendix. Now included new members, Pondanna and Moonaree Dacite Members, formerly referred to as 'black dacite" and "black (Yardea) dacite". Of Gawler Range Volcanics||||||
20845|Yardea Dacite|24356|5|Briefly described|p1593 Fig. 1|||Conformably overlies Eucarro Rhyolite.  Geological Province: Gawler Craton.||||||
20845|Yardea Dacite|24474|5|Briefly described|p36 Fig.1|||Of the Galwer Range Volcanics.  Geological Province: Gawler Craton.||||||
20845|Yardea Dacite|24476|4|Described|p545|Calymmian|Calymmian|Of the Gawler Range Volcanics. Age: 1592 +/- 3 Ma (U-Pb). Exposed Thickness: 250 m. Geological Province: Gawler Craton.||||||
20845|Yardea Dacite|29838|2|Defined|p13|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
20845|Yardea Dacite|30984|2|Defined|p11|Proterozoic|Proterozoic|||||||
20845|Yardea Dacite|37461|6|Mentioned|p325|||||||||
20845|Yardea Dacite|39802|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
20845|Yardea Dacite|40241|6|Mentioned|p115|||||||||
20845|Yardea Dacite|40430|6|Mentioned|p3|||||||||
20845|Yardea Dacite|40644|6|Mentioned| p124 Fig. 3, p136|Mesoproterozoic||Age: 1530+/-166Ma, and 1529+/-35Ma (both on black dacite) - see table 4, p135.||||||13-AUG-08
20845|Yardea Dacite|41619|6|Mentioned|Map legend|Mesoproterozoic||||||||
20845|Yardea Dacite|41833|6|Mentioned|p585|||||||||
20845|Yardea Dacite|41953|6|Mentioned|p132|||||||||
20845|Yardea Dacite|41972|5|Briefly described|p374|||||||||
20845|Yardea Dacite|41974|4|Described|p409|||||||||
20845|Yardea Dacite|42095|6|Mentioned|p29|||||||||
20845|Yardea Dacite|42274|6|Mentioned|p460|||||||||
20845|Yardea Dacite|42283|6|Mentioned|Fig.5 P82|||||||||
20845|Yardea Dacite|42368|4|Described|p48|||U-Pb zircon age 1592+/-3 Ma. Upper most unit of Gawler Range Volcanics.||||||22-MAY-14
20845|Yardea Dacite|42466|5|Briefly described|Map Legend|||||||||
20845|Yardea Dacite|42475|4|Described|p16|||part of "younger" Gawler Range Volcanics||||||
20845|Yardea Dacite|42546|5|Briefly described|Map legend|Mesoproterozoic||||||||
20845|Yardea Dacite|42721|5|Briefly described|map legend|Carpentarian||||||||
20845|Yardea Dacite|42736|5|Briefly described|map legend|Mesoproterozoic||||||||
20845|Yardea Dacite|42777|5|Briefly described|p291|||||||||
20845|Yardea Dacite|42779|6|Mentioned|p283|||||||||
20845|Yardea Dacite|43052|4|Described|p115|||Of Gawler Range Volcanics.||||||30-SEP-08
20845|Yardea Dacite|43053|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of the Upper Gawler Range Volcanics. Acid volcanics.||||||
20845|Yardea Dacite|43071|6|Mentioned|p12|||||||||
20845|Yardea Dacite|43094|4|Described|Table 4.|||||||||
20845|Yardea Dacite|43258|5|Briefly described|Map Legend||Mesoproterozoic|||||||
20845|Yardea Dacite|43298|6|Mentioned|Map Legend||Mesoproterozoic|||||||
20845|Yardea Dacite|43650|6|Mentioned|p443|||||||||
20845|Yardea Dacite|43651|5|Briefly described|p431|||||||||
20845|Yardea Dacite|43652|6|Mentioned|p390|||||||||
20845|Yardea Dacite|43839|6|Mentioned|p29||Mesoproterozoic|Within upper Gawler Range Volcanics||||||12-JUL-16
20845|Yardea Dacite|50127|5|Briefly described|p47|Neoproterozoic III|Neoproterozoic III|Age: ca 580 Ma. Geological Province: Gawler Craton.||||||
20845|Yardea Dacite|50605|5|Briefly described|p(ii), 8.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Gawler Craton & Curnamona Province. Of the Upper Gawler Range Volcanics. Age: 1592 +/- 3Ma (U-Pb).||||||
20845|Yardea Dacite|60704|5|Briefly described|p687|Calymmian|Calymmian|Of the Gawler Range Volcanics. Age: 1592+/-3 Ma (Fanning et al., 2002)||||||
20845|Yardea Dacite|60953|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Age: 1592Ma. Of the Upper Gawler Range Volcanics. Dacite, rhyodacite.||||||
20845|Yardea Dacite|61108|5|Briefly described|map legend|Mesoproterozoic|Mesoproterozoic|Of the Gawler Range Volcanics, Upper. Age: 1592 Ma.||||||23-JUN-05
20845|Yardea Dacite|61565|5|Briefly described|p607, p611|Mesoproterozoic|Mesoproterozoic|Intensely shattered rock; displays small shatter cones from the Acraman-Bunyeroo impact event.  Age: 1592+/-3Ma (U-Pb zircon, Fanning et al 1988).||||||
20845|Yardea Dacite|61732|6|Mentioned|p40|||This Lake Acraman country rock.||||||07-FEB-11
20845|Yardea Dacite|62963|5|Briefly described|p28, p29|Mesoproterozoic|Mesoproterozoic|Of the Gawler Range Volcanics. Crystallisation age: 1592+/-3Ma. Geological povince: Gawler Craton.||||||21-DEC-06
20845|Yardea Dacite|64131|6|Mentioned|p1402 |||||Unit in Gawler Range Volcanics.||||
20845|Yardea Dacite|65390|5|Briefly described|p17, p26 Tb. 1|Calymmian|Calymmian|Gawler Range Volcanics Domain, Gawler Craton. Age of 1592 +/- 3 Ma (Fanning et al. 1988) given. Intruded by Granite,'Hiltaba'.||||||
20845|Yardea Dacite|65922|5|Briefly described|p6, p16, p17 Tb. 2, p19-23|Calymmian|Calymmian|Uppermost exposed unit of Gawler Range Volcanics. Has a U-Pb zircon age of 1592 +/- 3 Ma (Fanning et al. 1988). Intruded by unnamed porphyritic rhyolite to rhyodacite dykes also within the Gawler Range Volcanics, and Hiltaba Suite granite. Contains Pondanna Dacite Member? Basal black welded dacite, grading upwards into massive, highly porphyritic dacite to rhyodacite; xenolith-rich zones and abundant mafic enclaves. REE patterns imply common genesis with Eucarro Dacite and Nonning Rhyodacite. Geochemistry described in detail.||||||22-MAY-14
20845|Yardea Dacite|66302|6|Mentioned|p33|||||||||
20845|Yardea Dacite|66569|5|Briefly described|p859,|Calymmian|Calymmian|Of the Gawler Range Volcanics; 1592 +/-2 Ma; hosts the Acraman impact structure.||||||
20845|Yardea Dacite|67027|6|Mentioned|p350.|||Shattered samples from the Acraman impact site were studied for apatite fission track analysis; dated at 319 +/- 19 Ma.||||||
20845|Yardea Dacite|67028|5|Briefly described|p362, p364 Tb.1, p373|Calymmian|Calymmian|Different unit from Black Yardea Dacite or just different sample site? Information on magnetic characteristics presented. Kokatha-type.||Gawler Range Volcanics||||24-APR-12
20845|Yardea Dacite|67900|5|Briefly described|p20-21|Mesoproterozoic|Mesoproterozoic|Gawler Craton. The most extensive unit of the Upper Gawler Range Volcanics; exposed over 12,000 km2, erupted volume of 3,000 km3.|1592 +/- 3 Ma (Fanning et al., 1988).|Upper Gawler Range Volcanics.||||
20845|Yardea Dacite|67909|5|Briefly described|p124, 130-131, 141|Mesoproterozoic|Mesoproterozoic|Allen and McPhie (2002).|1592-1591 Ma.|Gawler Range Volcanics.||Correlated with Chandabooka Dacite.||
20845|Yardea Dacite|68126|5|Briefly described|p21||||1592 +/- 3 Ma (U-Pb zircon: Fanning et al., 1986).|Gawler Range Volcanics.||||
20845|Yardea Dacite|69649|5|Briefly described|p16-17, p34, p51|Mesoproterozoic|Mesoproterozoic|Extensive unit.|1592 +/- 3 Ma; U-Pb zircon (Fanning et al., 1988).|Unit in Gawler Range Volcanics.||||26-FEB-15
20845|Yardea Dacite|70659|5|Briefly described|p6 fig 2, p8|Mesoproterozoic|Mesoproterozoic|Gawler Ranges.||Upper Gawler Range Volcanics.|Includes Moonaree Dacite Member, Pondanna Dacite Member.|||
20845|Yardea Dacite|70789|6|Mentioned|p321|||AFT results tabulated; central age 354 +/- 13 Ma.||||||
20845|Yardea Dacite|70816|5|Briefly described|p4-5|||Gawler Ranges region.||Unit of upper Gawler Range Volcanics.|Includes Pondanna and Moonaree Dacite members|Equivalent to Carnding Rhyodacite and Chandabooka Dacite.||
20845|Yardea Dacite|71129|5|Briefly described|p88|||Geological Province: Gawler Craton.||||||
20845|Yardea Dacite|71317|4|Described|p1, p20, p26, p54, p56|Mesoproterozoic|Mesoproterozoic|Occupies a large area of the central and northern Gawler Ranges. Mapped by Blissett et al., 1988 who seperated it into a thin black sparsely porphyritic dacite and an overlying red-brown massive dacite. Recent mapping by Allen et al., 2003 subdivided it into its two current members. See alsop85-p86, p98-p99, p104, p113, p176.||Gawler Range Volcanics|Includes the Pondanna Dacite Member, Moonaree Dacite Member and the Yartoo Volcaniclastics.|Locally overlies the Mount Friday Formation and overlies the Eucarro Rhyolite.||
20845|Yardea Dacite|71559|4|Described|p16, p19-20, p22|Mesoproterozoic|Mesoproterozoic|Geological province: Gawler Craton.||Unit of Upper Gawler Range Volcanics.|Includes Pondanna and Moonaree Dacite members.|||19-JUN-19
20845|Yardea Dacite|71560|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Six facies are mapped separately, three in each of the two Members.||Upper Gawler Range Volcanics.|Pondanna, Moonaree, Dacite Members.||Dacites.|16-APR-18
20845|Yardea Dacite|72065|5|Briefly described|p105-106|Calymmian|Calymmian|Geological province: Gawler Craton. Also shown as Yardea Dacite Formation.||Unit of Gawler Range Volcanics.|Includes Moonaree and Pondanna dacite members.|||
20845|Yardea Dacite|72089|5|Briefly described|p2|||Gawler Craton.||Gawler Range Volcanics, upper|Includes the Pondanna Dacite Member and the Moonaree Dacite Member.||Dacitic lava.|
20845|Yardea Dacite|72090|6|Mentioned|p12|||Gawler Craton.||Gawler Range Volcanics, Upper|Includes the Pondanna Dacite Member and Moonaree Dacite Member.|||
20845|Yardea Dacite|72459|5|Briefly described|p17-19, p23, p46-47|Mesoproterozoic|Mesoproterozoic|Large volume unit interpreted to be ignimbritic in origin with minor interbedded lavas. Part of the 'mature' phase of the Gawler Range Volcanism.||Gawler Range Volcanics|||Dacite with mafic to intermediate inclusions.|
20845|Yardea Dacite|72462|6|Mentioned|p8-9|||Contains abundant (up to 30 volume %) lithic clasts to megablocks ranging from less than one metre to 50 m in diameter, including granite, monzonite, pegmatite, and felsic and mafic volcanics. These mostly have sharp boundaries but some are diffuse.||Gawler Range Volcanics|Pondanna Dacite Member, Moonaree Dacite Member|||
20849|Yardinna Claystone|30807|6|Mentioned|p101|||Suggested map symbol||||||
20849|Yardinna Claystone|31699|4|Described|p132|||Pliocene||||||
20849|Yardinna Claystone|40926|6|Mentioned|Table 3|||||||||
20849|Yardinna Claystone|44133|5|Briefly described|p190 Fig. 10.30|Middle Miocene|Early Miocene|Geoloigcal Province: Lake Eyre Basin.||||||
20849|Yardinna Claystone|44658|14|Not recorded|map legend|||?U.Cainozoic. (G53-15).||||||
20849|Yardinna Claystone|67462|5|Briefly described|Map legend.|Miocene|Miocene|Tirari Sub-basin, Lake Eyre Basin.||||||
20849|Yardinna Claystone|68715|6|Mentioned|p30 Fig.5|Serravallian|Burdigalian|Tirai and northern Callabonna sub basins, Lake Eyre Basin.||||||
20849|Yardinna Claystone|69019|5|Briefly described|p105 Fig.25.|Miocene|Miocene|Tirari Sub-basin.||||Overlies Etadunna Formation.||
20849|Yardinna Claystone|69023|6|Mentioned|p108|Miocene|Miocene|Tirari Sub-basin, Lake Eyre Basin.||||||
20849|Yardinna Claystone|70336|5|Briefly described|Map legend|Miocene|Miocene||||||Pale green and brown, dolomitic claystone.|
20856|Yarloo Shale|23250|5|Briefly described|p1124 Fig.2||Neoproterozoic III|Correlate of Bunyeroo Formation (Wilpena Group) and Pertatataka Formation.||||||
20856|Yarloo Shale|23282|6|Mentioned|p89||Neoproterozoic|Age: 588+/-35Ma.||||||
20856|Yarloo Shale|23287|6|Mentioned|Fig.2|||Age: Upper Ediacaran.  Of Stuart Shelf.||||||18-APR-13
20856|Yarloo Shale|23445|6|Mentioned|p435|||||||||
20856|Yarloo Shale|23818|5|Briefly described|p76|||Equivalent of the Bunyeroo Formation. Overlying unit: Andamooka Limestone.||||||
20856|Yarloo Shale|23913|4|Described|p108, p110 Fig. 2|Adelaidean|Adelaidean|Geological province: Stuart Shelf. Of the Wilpena Group.  Age: 593 +/- 35 Ma.  Underlying Unit: Tent Hill Formation.||||||
20856|Yarloo Shale|24476|4|Described|p547 Fig.4|Vendian|Vendian|Overlies the Tent Hill Formation. Geological Province: Stuart Shelf.||||||
20856|Yarloo Shale|30807|6|Mentioned|p102|||Suggested map symbol||||||
20856|Yarloo Shale|31539|6|Mentioned|p56|||||||||
20856|Yarloo Shale|34535|6|Mentioned|p76|||||||||
20856|Yarloo Shale|35548|6|Mentioned|p17|||||||||
20856|Yarloo Shale|37461|6|Mentioned|Table 5.I|||||||||
20856|Yarloo Shale|38157|6|Mentioned|Table V|||||||||
20856|Yarloo Shale|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Marinoan||||||
20856|Yarloo Shale|39352|6|Mentioned|Map legend|Adelaidean|Adelaidean|Marinoan||||||
20856|Yarloo Shale|39808|6|Mentioned|p223|||||||||
20856|Yarloo Shale|40852|6|Mentioned|Fig.3.7|||||||||
20856|Yarloo Shale|41005|6|Mentioned|p419|||||||||
20856|Yarloo Shale|41429|5|Briefly described|p230|||||||||
20856|Yarloo Shale|41493|6|Mentioned|Table 1|||||||||
20856|Yarloo Shale|42222|5|Briefly described|p19|||||||||
20856|Yarloo Shale|42247|6|Mentioned|p9|||||||||
20856|Yarloo Shale|42465|5|Briefly described|Map Legend|||||||||
20856|Yarloo Shale|42469|5|Briefly described|p25|||||||||
20856|Yarloo Shale|42600|5|Briefly described|Table 1 P2|||||||||
20856|Yarloo Shale|42777|5|Briefly described|p292|||||||||
20856|Yarloo Shale|43052|5|Briefly described|p194,table 6.1|||of Wilpena  Group.Age of 588+/-35 Ma||||||
20856|Yarloo Shale|44133|5|Briefly described|p24|||Underlies: Andamooka Limestone.||||||
20856|Yarloo Shale|44689|14|Not recorded|map legend||Late Adelaidean|Andamooka. (H53-12). Uppermost Adelaidean.||||||
20856|Yarloo Shale|60955|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Purple Shales. Equivalent to Bunyeroo Formation. Of the Wilpena Group.||||||13-APR-05
20856|Yarloo Shale|61732|5|Briefly described|p4 Fig. 3|Marinoan|Marinoan|Of the Wilpena Group. Age: 588+/-35Ma. Geological Province: Adelaide Rift Complex/Stuart Shelf.||||||07-FEB-11
20856|Yarloo Shale|62453|4|Described|p12 Fig. 8|Ediacaran|Ediacaran|Geological Province: Adelaide Rift Complex/Stuart Shelf. Age: 588 +/- 35Ma. Of the Wilpena Group.||||||18-APR-13
20856|Yarloo Shale|65365|5|Briefly described|p10 Fig. 4|||Of Wilpena Group. Rb-Sr age 588 +/- 35 Ma (Webb, 1980).||||||19-MAR-12
20856|Yarloo Shale|65366|5|Briefly described|p23 Fig. 3|Ediacaran|Ediacaran|Of Wilpena Group. Rb-Sr age 588 +/- 35 Ma (Webb, 1980).||||||19-MAR-12
20856|Yarloo Shale|65892|6|Mentioned|p32.|Ediacaran|Ediacaran|Adelaide Geosyncline. Last major Neoproterozoic transgression, reaching the Stuart Shelf but not the eastern Curnamona Province.||||||
20856|Yarloo Shale|66569|5|Briefly described|p861,|Ediacaran|Ediacaran|Equivalent to Bunyaroo Formation; Rb-Sr isochron age of 588 +/- 35 Ma.||||||
20856|Yarloo Shale|67030|5|Briefly described|p409|Ediacaran|Ediacaran|Stuart Shelf area.|593 +/- 32 Ma (Rb-Sr, Compston et al. 1987)|||equivalent to the Bunyeroo Formation||
20856|Yarloo Shale|69019|6|Mentioned|p58.|||||||||
20856|Yarloo Shale|70082|6|Mentioned|p2|Ediacaran|Ediacaran|Stuart Shelf. Contains red beds.||||||
20856|Yarloo Shale|70334|5|Briefly described|p56|||Geological province: Gawler Craton. Of Stuart Shelf.||||Underlain by Tent Hill Formation.||
20856|Yarloo Shale|70406|5|Briefly described|p125, 121|||||Of Aruhna Subgroup.||Conformably overlies Simmens Quartzite. Unconformably overlain by Wearing Dolomite.||
20856|Yarloo Shale|70407|6|Mentioned|p110|||Stuart Shelf. Outcrops at Bill's Lookout previously interpreted as this unit. Now, in part, interpreted as lateral equivalent of Wearing Dolomite.||||||
20856|Yarloo Shale|71129|5|Briefly described|p128|Ediacaran|Ediacaran|Of northern Stuart Shelf.||Unit of Wilpena Group.||Underlain by Tent Hill Formation.||
20856|Yarloo Shale|74367|5|Briefly described|p7 Fig.6, p8, p11, p19|Ediacaran|Ediacaran|Stuart Shelf.|588+/-35 Ma Rb-Sr whole rock depositional age|Aruhna Subgroup||Equivalent to Bunyeroo Formation||
20893|Yarrawurta Shale|23250|5|Briefly described|p1124 Fig.2||Early Cambrian|Age: Stage 4 of Early Cambrian. Correlate of Wirrealpa Limestone.||||||
20893|Yarrawurta Shale|30051|6|Mentioned|Fig.11|||||||||
20893|Yarrawurta Shale|30807|6|Mentioned|p102|||Suggested map symbol||||||
20893|Yarrawurta Shale|33474|6|Mentioned|Fig.3|||||||||
20893|Yarrawurta Shale|35835|6|Mentioned|p208|||||||||
20893|Yarrawurta Shale|39352|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
20893|Yarrawurta Shale|40852|6|Mentioned|Fig.3.7|||||||||
20893|Yarrawurta Shale|41493|6|Mentioned|Table 1|||||||||
20893|Yarrawurta Shale|42011|6|Mentioned|Fig.3 P458|||||||||
20893|Yarrawurta Shale|42247|6|Mentioned|p5|||||||||
20893|Yarrawurta Shale|42469|5|Briefly described|p27|||Andamooka, SH53-12||||||
20893|Yarrawurta Shale|43052|5|Briefly described|Table 2.1|||||||||
20893|Yarrawurta Shale|43053|5|Briefly described|Map Legend|Cambrian|Cambrian|Shallow marine to terrestrial redbeds, peritidal to marine limestone.||||||25-MAY-05
20893|Yarrawurta Shale|43258|5|Briefly described|Map Legend||Cambrian|||||||
20893|Yarrawurta Shale|43298|6|Mentioned|Map Legend||Cambrian|||||||
20893|Yarrawurta Shale|44133|5|Briefly described|p4 Fig. 7.2, 27|Early Cambrian|Early Cambrian|Geological Province: Arrowie Basin. Overlies: upper Andamooka Limestone. Maximum Thickness: 90m.||||||03-MAY-13
20893|Yarrawurta Shale|60953|5|Briefly described|Map Legend|Cambrian|Cambrian|Geological Province: Stuart Shelf.||||||
20893|Yarrawurta Shale|60955|5|Briefly described|Map Legend|Cambrian|Cambrian|Red-brown, purple and green shales and siltstones. Billy Creek Formation is equivalent.||||||13-APR-05
20893|Yarrawurta Shale|61108|5|Briefly described|map legend|Cambrian|Cambrian|Shallow marine to terrestrial redbeds; peritidal to marine limestone. Geological Province: Stuart Shelf.||||||03-JUN-05
20893|Yarrawurta Shale|65686|6|Mentioned|p413|Early Cambrian|Early Cambrian|Arrowie Basin.|||||Red beds.|07-MAY-12
20893|Yarrawurta Shale|67536|5|Briefly described|Map Legend|Stage 2|Stage 2||ca. 523 +/- 2 Ma||||Shallow marine to terrestrial redbeds, peritidal to marine limestone|
20962|Yerelina Subgroup|22510|1|Redefined|table1p37,41|||Age: Marinoan. Redefined to include the entire Marinoan glacial succession, including Elatina Formation and Whyalla Sandstone as well as previously defined constituents.  Overlies, mostly disconformably, the Upalinna Subgroup.||||||11-SEP-07
20962|Yerelina Subgroup|22631|6|Mentioned|p178|||Age: Marinoan||||||08-JUL-13
20962|Yerelina Subgroup|22772|5|Briefly described|Table13.1|Neoproterozoic III|Neoproterozoic III|||||||
20962|Yerelina Subgroup|22857|5|Briefly described|Tb. 13.1 (insert p70-71)|Marinoan|Marinoan|Of the Umberatana Group. Age: >590Ma.||||||
20962|Yerelina Subgroup|23351|5|Briefly described|283|Neoproterozoic|Neoproterozoic|||||||
20962|Yerelina Subgroup|23806|5|Briefly described|p1122 Fig. 1|Neoproterozoic|Neoproterozoic|||||||
20962|Yerelina Subgroup|23913|5|Briefly described|p108|||Geological Province: Adelaide Geosyncline.  Max. thickness: > 1500m.||||||
20962|Yerelina Subgroup|24175|4|Described|p13|Neoproterozoic III|Neoproterozoic|Of the Umberatana Group.  Informally referred to as Upper Umberatana Group of the eastern area.  Comprises Fortress Hill Formation and Mount Curtis Tillite.  Overlies Amberoona Formation.||||||11-SEP-07
20962|Yerelina Subgroup|24321|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Umberatana Group.||||||11-SEP-07
20962|Yerelina Subgroup|24546|5|Briefly described|p2 - 3 Fig.2|Neoproterozoic|Neoproterozoic|Of Umberatana Group. Geological Province: Adelaide Fold Belt.||||||16-JAN-08
20962|Yerelina Subgroup|30621|6|Mentioned|p501|||Glacigenic||||||08-JUL-13
20962|Yerelina Subgroup|35255|6|Mentioned|p13|||||||||
20962|Yerelina Subgroup|36137|5|Briefly described|p4|||||||||
20962|Yerelina Subgroup|36898|6|Mentioned|p181|||See also P196.||||||
20962|Yerelina Subgroup|37238|6|Mentioned|Table 1|||||||||
20962|Yerelina Subgroup|37461|5|Briefly described|p342|||||||||
20962|Yerelina Subgroup|37932|3|Fully described|p545|||See also p544.||||||11-SEP-07
20962|Yerelina Subgroup|38110|6|Mentioned|p3|||||||||
20962|Yerelina Subgroup|38157|6|Mentioned|Table IV|||||||||
20962|Yerelina Subgroup|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Marinoan||||||
20962|Yerelina Subgroup|39352|6|Mentioned|Map legend|Adelaidean|Adelaidean|Marinoan||||||
20962|Yerelina Subgroup|40911|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
20962|Yerelina Subgroup|41401|6|Mentioned|Table 4|||||||||
20962|Yerelina Subgroup|41405|4|Described|p197|||Mention p174.||||||11-SEP-07
20962|Yerelina Subgroup|41500|6|Mentioned|Fig.1|||||||||
20962|Yerelina Subgroup|41526|6|Mentioned|p3|||||||||
20962|Yerelina Subgroup|42098|5|Briefly described|Fig.1 P52|||||||||
20962|Yerelina Subgroup|42109|5|Briefly described|Fig.1 P19|||||||||
20962|Yerelina Subgroup|42222|4|Described|p18|||||||||
20962|Yerelina Subgroup|42238|6|Mentioned|Table 1 P74|||||||||
20962|Yerelina Subgroup|42239|6|Mentioned|p149|||||||||
20962|Yerelina Subgroup|42240|6|Mentioned|Fig.2 P165|||||||||
20962|Yerelina Subgroup|42272|6|Mentioned|p403|||||||||
20962|Yerelina Subgroup|42542|5|Briefly described|p7, p8|||||||||
20962|Yerelina Subgroup|42720|5|Briefly described|map legend|Marinoan||||||||
20962|Yerelina Subgroup|42813|4|Described|p21|||Of the Umberatana Group.||||||11-SEP-07
20962|Yerelina Subgroup|43052|5|Briefly described|p190,Table 6.1|||of Umberatana Group||||||
20962|Yerelina Subgroup|45155|6|Mentioned|p28|||Correlation||||||
20962|Yerelina Subgroup|60953|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Glaciomarine diamictite, sandstone and siltstone, aeolian sandstone. Geological Province: Stuart Shelf.||||||
20962|Yerelina Subgroup|60959|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Of the Umberatana Group.||||||
20962|Yerelina Subgroup|61108|5|Briefly described|map legend|Adelaidean|Adelaidean|Glaciomarine diamictite, sandstone and siltstone; aeolian sandstone. Geological Province: Stuart Shelf.||||||
20962|Yerelina Subgroup|61238|5|Briefly described|p44 Fig. 1|Neoproterozoic|Neoproterozoic|Of the Umberatana Group.||||||
20962|Yerelina Subgroup|61732|5|Briefly described|p28 Fig. 13|Marinoan|Marinoan|Of Umberatana Group. Includes Fortress Hill Formation, Gumbowie Arkose, Pepuarta Tillite, Elatina Formation, Grampus Quartzite and Ketchowla Siltstone. Geological Province: Adelaide Rift Complex.||||||07-FEB-11
20962|Yerelina Subgroup|62592|5|Briefly described|p50 Table 5.1, p59.|Marinoan|Marinoan|Adelaide Geosyncline.||Unit in Umberatana Group.|Includes Elatina Formation.|Disconformably overlies Upalinna Subgroup.||
20962|Yerelina Subgroup|62903|5|Briefly described|p729, p730 Fig.1|Marinoan|Marinoan Marinoan|glaciation||||interpreted as equivalent with Olympic Formation (Walter et al. 2000); overlies Upalinna Subgroup, Upper.||
20962|Yerelina Subgroup|63458|6|Mentioned|p897 Fig.19. |Cryogenian|Cryogenian|||Unit in Umberatana Group.|Includes Elatina Formation.|||
20962|Yerelina Subgroup|63489|5|Briefly described|Map legend|Adelaidean|Adelaidean|Glacigenic, pebbly siltstone and sandstone, local diamictite and conglomerate. New South Wales equivalent is Teamsters Creek Subgroup.||||||10-SEP-07
20962|Yerelina Subgroup|64801|6|Mentioned|p110 Fig.2, p111|Neoproterozoic|Neoproterozoic|Adelaide Rift Complex. Marinoan glacials.||Umberatana Group.||||
20962|Yerelina Subgroup|64846|5|Briefly described|p198|Cryogenian|Cryogenian|Marinoan glaciation.||Of the Umberatana Group.|Includes the Elatina Formation.|||
20962|Yerelina Subgroup|65493|5|Briefly described|p910, p909 Fig 2|Cryogenian|Cryogenian|Of Umberatana Group. Includes Elatina Formation. Unconformably overlies the Upalinna Subgroup. Upper boundary defined by an erosional surface formed by glaciation events.||||||
20962|Yerelina Subgroup|66569|5|Briefly described|p860, p861 fig.2,|||Glaciogenic units. Disconformably to unconformably underlies Nuccaleena Formation. Includes Elatina Formation.||||||
20962|Yerelina Subgroup|67180|6|Mentioned|p601 Fig.1|Cryogenian|Cryogenian|Marinoan age.||Unit in Umberatana Group|Includes Elatina Formation|||
20962|Yerelina Subgroup|67870|5|Briefly described|p9|Neoproterozoic|Neoproterozoic|Adelaide Rift System.||Umberatana Group.|Elatina Formation.|||
20962|Yerelina Subgroup|67979|5|Briefly described|p528, p542|Marinoan|Marinoan|Early Marinoan-aged glacial successions (Coats and Blissett 1971). No direct geochronological ages.||uppermost successsion in Umberatana Group||overlies Upalinna Subgroup||
20962|Yerelina Subgroup|68269|6|Mentioned|p674|||Adelaide Geosyncline.|||Elatina Formation|Unconformably overlain by Seacliff Sandstone (Wilpena Group).||
20962|Yerelina Subgroup|68274|6|Mentioned|p13|Neoproterozoic|Neoproterozoic|||||||
20962|Yerelina Subgroup|69019|5|Briefly described|p41, p51-54.|Neoproterozoic|Neoproterozoic|Redefined by Preiss (1998) to include the entire Marinoan glacial succession within the Umberatana Group.||Unit in Umberatana Group.|Includes Fortress Hill Formation, Gumbowie Arkose, Mount Curtis Tillite, Balparana Sandstone and Ketchowla Siltstone.||Siltstone, sandstone and variably calcareous diamictite.|
20962|Yerelina Subgroup|70031|5|Briefly described|p245|Cryogenian|Cryogenian|Adelaide Geosyncline. Glaciogenic succession marking the start of the Elatina glaciation.||Unit of Umberatana Group.|Incldues Elatina Formation.|Uppermost unit of Umberatana Group. Overlain disconformably to unconformably by  Wilpena Group/Nuccaleena Formation. Underlain by Upalinna Subgroup/Trezona Formation and Yaltipena Formation.||
20962|Yerelina Subgroup|70334|5|Briefly described|p20,29,38,47,53,54|||Geological province: Gawler Craton. Of Adelaide Geosyncline and Stuart Shelf.||Unit of Umberatana Group.|Includes Whyalla Sandstone and Elatina Formation.|||
20962|Yerelina Subgroup|70384|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Adelaide Geosyncline.  Age shown more specifically as Marinoan [Cryogenian].||of Umberatana Group.|Includes Fortress Hill, Elatina Formations; Gumbowie Arkose; Mount Curtis Tillite; Balparana Sandstone.|Unconformably overlies Upalinna Subgroup. Is overlain unconformably by Sandison Subgroup (Wilpena Group).|Greyish to greenish, variably calcareous, siltstone, sandstone and diamictite.|23-JAN-19
20962|Yerelina 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 Upalinna Subgroup.|Sandstone, siltstone and conglomerate.|
20962|Yerelina Subgroup|71129|4|Described|p107,109,111,118,138,184,187,208,225,227|Cryogenian|Cryogenian|Of Stuart Shelf. Deposited during ensuing glacio-eustatic sea-level rise after Sturt Glaciation. Historically difficult to distinguish between Whyalla Sandstone and Yudnapinna Beds-Wilmington Formation/Upalinna Subgroup in the southwestern Stuart Shelf, and therefore sandstone successions intersected in drillholes between Tapley Hill and Tent Hill formations are variably interpreted as Whyalla sandstone or undifferentiated Umberatana Group. See also p1, p15.||Unit of Umberatana Group.|Includes Whyalla Sandstone.|Overlies the Upalinna Subgroup.|Sandstone, siltstone and conglomerate; undifferentiated.|13-NOV-19
20962|Yerelina Subgroup|71130|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|||Umberatana Group.|||Sandstone, siltstone and conglomerate.|
20962|Yerelina Subgroup|71131|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|||Umberatana Group.|||Sandstone, siltstone and conglomerate.|
20962|Yerelina Subgroup|71895|6|Mentioned|APP4. p4, |||Punt Hill Region.||||||
20962|Yerelina Subgroup|72090|5|Briefly described|p34, p37, p95|||Gawler Craton.|||||Pale reddish brown to greyish brown, fine- to medium-grained, moderately to well sorted, convolute bedding, flaser bedding, laminations, interbedded shale and sandstone.|
20962|Yerelina Subgroup|72456|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Marree 1:250k map sheet.|||||Siltstone, sandstone and diamictite.|
20962|Yerelina Subgroup|73093|5|Briefly described|map legend|Neoproterozoic|Neoproterozoic||||||Siltstone; sandstone; diamictite.|09-DEC-21
20962|Yerelina Subgroup|73188|5|Briefly described|p315-316|Neoproterozoic|Neoproterozoic|Marinoan.||Umberatana Group|Reynella Siltstone Member||Glacials.|
20962|Yerelina Subgroup|73234|6|Mentioned|p6|||||Umberatana Group|Whyalla Sandstone|||
20962|Yerelina Subgroup|73236|6|Mentioned|p36, p38|Ediacaran|Ediacaran|Marine sedimentary rocks.||Umberatana Group, Heysen Supergroup|Reynella Siltstone Member, Elatina Formation|Underlain by Wilmington Formation (Upalinna Subgroup). [Unconformably] overlain by Seacliff Sandstone (Sandison Subgroup, Wilpena Group).||
20962|Yerelina Subgroup|74367|5|Briefly described|p7 Fig.6, p8, p19|Cryogenian|Cryogenian|Previously part of the now superseded 'Willochra Subgroup'.|||Fortress Hill Formation, Elatina Formation, Whyalla Sandstone|||
20964|Yerila Granite|22631|6|Mentioned|p176|Calymmian|Calymmian|||||||
20964|Yerila Granite|22795|5|Briefly described|p69|Mesoproterozoic|Proterozoic|||||||
20964|Yerila Granite|23394|5|Briefly described|Map legend|Proterozoic|Proterozoic|||||||
20964|Yerila Granite|23775|6|Mentioned|p728|||||||||22-SEP-09
20964|Yerila Granite|23804|6|Mentioned|p17|||||||||
20964|Yerila Granite|23818|6|Mentioned|p37|||||||||
20964|Yerila Granite|24045|5|Briefly described|p554 Table 1|Mesoproterozoic|Paleoproterozoic|||||||07-NOV-08
20964|Yerila Granite|24197|5|Briefly described|p75 Tb. 8.1|Mesoproterozoic|Mesoproterozoic|Age: 1560Ma.||||||07-FEB-11
20964|Yerila Granite|24546|5|Briefly described|p2 - 5|Devonian|Devonian|Age: ~400 Ma (K-Ar; Webb, 1976). Geological Province: Adelaide Fold Belt.||||||
20964|Yerila Granite|30177|2|Defined|p125|Carpentarian|Carpentarian|See also p39.Prob. Carpentarian. Type locality: Mudnawatana Creek, 1.6 miles west-northwest of Birthday Well, lat. 29degrees54'55"S long. 139degrees31'09"E.||||||24-NOV-22
20964|Yerila Granite|30807|6|Mentioned|p103|||Suggested map symbol||||||
20964|Yerila Granite|34537|6|Mentioned|p37|||||||||
20964|Yerila Granite|38068|6|Mentioned|p67|||||||||
20964|Yerila Granite|42602|5|Briefly described|p20,p19|||||||||
20964|Yerila Granite|42624|4|Described|p23|||||||||
20964|Yerila Granite|43052|5|Briefly described|p153|||||||||
20964|Yerila Granite|50605|5|Briefly described|p(ii), 1.4, 10.1, 10.2, Table 1.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Gawler Craton & Curnamona Province. Of the Moolawatana Suite (Babbage supersuite). Age: 1556 +/- 15Ma (U-Pb).||||||30-AUG-04
20964|Yerila Granite|62962|5|Briefly described|p2284 Fig. 2|Mesoproterozoic|Mesoproterozoic|Age: 1551+/-38Ma (Johnson, 1980. U/Pb SHRIMP). Geological Province: Mount Painter Province.||||||07-FEB-11
20964|Yerila Granite|65455|5|Briefly described|p12|Mesoproterozoic|Mesoproterozoic|Mount Babbage Inlier. See also informal Yerila granite, p9. Has uranium abundances of greater than 100 parts per million.||Of Babbage Supersuite.|||A metaluminous, fractionated granite.|09-MAY-12
20964|Yerila Granite|65925|5|Briefly described|p12.|Early Mesoproterozoic|Early Mesoproterozoic|Babbage Inlier. Very high (116 ppm) uranium content.||||||
20964|Yerila Granite|66302|6|Mentioned|p50, p78|Calymmian|Calymmian|Moolawatana Domain, Curnamona Province.|1558 +/- 3 Ma (SHRIMP, Fraser and Neumann, 2010)|Moolawatana Suite||||
20964|Yerila Granite|68068|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Curnamona Province.|1558 +/- 10 Ma (U-Pb zircon).|Unit in Moolawatana Suite.|||Lineated tabular feldspar phenocrystic granite, gneissic, usually melanocratic, grey to dark grey, enriched in REE; composed of microcline laths, albite, quartz, biotite, muscovite with accessory apatite, zircon and tourmaline.|
20964|Yerila Granite|68205|5|Briefly described|p84-85,88-90,92, p94|||Geological province: Curnamona Province. Occurs in the Mt Babbage Inlier only. Geochemical analysis provided from p88-92. Nd isotope analysis on p92-94. U-Pb zircon geochronology on p94-99.||Unit of Moolawatana Suite.|||Greyish granite with large K-feldspar crystals.|02-JUL-19
20964|Yerila Granite|69019|5|Briefly described|p27-30 Figs.7-10, p163.|Calymmian|Calymmian|Geochemistry is described. Highly enriched in REE.|c.1555 Ma.|Unit in Moolawatana Suite.||||
20964|Yerila Granite|69023|4|Described|p23-28, p37-42, p49, p52, p64, p77|||See also p145-146, p158, p162, p189. Coats and Blissett (1971). Mount Babbage and Mount Painter Inliers. Middle level emplacement. Geochemistry detailed. Highly enriched in REE: thus quite radioactive and hence unsuitable for interior building stone. Major element abundances are similar to Mount Neill Granite. Xenoliths of this unit occur in Wattleowie and Terrapinna Granites. Locally hydrothermally altered.|1556 +/- 10 Ma U-Pb zircon (Johnson, 1980).|Unit in Moolawatana Suite.||Is intruded by Wattleowie and Terrapinna Granites and Mudnawatana Tonalite.|Characteristic parallel long white microcline laths and phenocrysts in a dark grey to black matrix of quartz, microcline and sodic-albite. Texture and mineralogy have been altered by dynamic metamorphism. Unusually rich in REE.|
20964|Yerila Granite|69562|5|Briefly described|p669, p670 Tb.5, p673 Fig.5, p683-684|||Consistently mis-spelt as Yerilla. Mount Babbage Inlier. Contains 4 to 270 ppm U: excellent source of leachable U. Has intensive metasomatic overprints.|1558 +/- 4 Ma (Fraser and Neumann, 2010).||||Medium- to coarse-grained. Contains uraninite and other U-bearing accessory minerals; extreme enrichment in REE.|
20964|Yerila Granite|70384|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Strong actinolite alteration in an area NW of Birthday Well. A similar TIMS age of 1556 +/- 10 Ma is also given.|1558 +/- 4 Ma (SHRIMP U-Pb zircon).||||Lineated tabular feldspar phenocrystic granite, gneissic, usually melanocratic, grey to dark grey, enriched in REE; composed of microcline laths, albite, quartz, biotite, muscovite, with accessory apatite, zircon and tourmaline.|
20964|Yerila Granite|71531|14|Not recorded|p10||Carpentarian|||||||
20964|Yerila Granite|72459|4|Described|p63, p66, p69, p73, p94-99|Mesoproterozoic|Mesoproterozoic|Forms sub""group"" 2a of this report along with a smaller dark, spotted granite mapped as undifferentiated granitoid at the contact between the Box Bore and Terapinna granites. Outcrops along the southern margin of the Mt Babbage inlier. Chemistry is discussed in some detail. Field relationships suggest this is the oldest member of the Moolawatana Suite.|1556 +/- 10 Ma (U-Pb zircon, Fanning, 1995)|Moolawatana Suite||Intruded by the Terrapinna Granite.|Lineated to gneissic grey granite with tabular feldspars.|
20964|Yerila Granite|73061|5|Briefly described|p1067, p1069, p1071-1072, p1075-1077|Calymmian|Calymmian|Mount Painter Province, Mount Babbage Inlier. Most radioactive and highest heat producing granite in the province. U-Pb zircon crystallisation age of 1556 +/- 6 Ma (Johnson, 1980), SHRIMP U-Pb zircon age of 1558 +/- 4 Ma (Fraser and Neumann, 2010). Mean eHf value of +1.4 +/- 1.3. Intruded by lamprophyres (1520 +/- 9 Ma and 1521 +/- 13 Ma) previously referred to as microgranular enclaves (Kromkhun and Foden, 2009), and crosscut by basaltic andesite dyke (1520 +/- 13 Ma) from a later stage of magmatism. Location in text includes p1068 Fig.1, p1070 Tb.1, Fig.2, p1073 Fig.3, p1074 Fig.4.|1562 +/- 26 Ma U-Pb LA-ICPMS, 1556 +/- 6 Ma||||Coarse- to medium-grained, inequigranular and locally gneissic granite. Includes pale grey, porphyric granite with tabular feldspar phenocrysts.|
21049|Yudnamutana Subgroup|22510|1|Redefined|table1p37,38,41|||Age: Sturtian. Redefined name, returns to the original concept of the unit. Disconformably overlain by Nepouie Subgroup.||||||13-FEB-08
21049|Yudnamutana Subgroup|22631|6|Mentioned|p177|Cryogenian|Cryogenian|Sturtian in age||||||
21049|Yudnamutana Subgroup|22772|5|Briefly described|Table13.1|Cryogenian|Cryogenian|||||||
21049|Yudnamutana Subgroup|22857|5|Briefly described|Tb. 13.1 (insert p70-71)|Sturtian|Sturtian|Of the Umberatana Group. Age: <700Ma.||||||
21049|Yudnamutana Subgroup|23477|5|Briefly described|p49 Fig 3|Neoproterozoic|Neoproterozoic|Geological Province: Curnamona Province.||||||
21049|Yudnamutana Subgroup|23806|5|Briefly described|p1122 Fig. 1|Neoproterozoic|Neoproterozoic|||||||
21049|Yudnamutana Subgroup|24175|5|Briefly described|p12|Neoproterozoic|Neoproterozoic|Of Umberatana Group.  Includes the Bolla Bollana Tillite.||||||
21049|Yudnamutana Subgroup|24321|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of the Umberatana Group.||||||11-SEP-07
21049|Yudnamutana Subgroup|24546|5|Briefly described|p2 - 3 Fig.2|Neoproterozoic|Neoproterozoic|Of Umberatana Group. Geological Province: Adelaide Fold Belt.||||||16-JAN-08
21049|Yudnamutana Subgroup|30178|6|Mentioned|p19|||||||||
21049|Yudnamutana Subgroup|30621|6|Mentioned|p501|||Glaciogenic||||||
21049|Yudnamutana Subgroup|30810|6|Mentioned|p4|||||||||
21049|Yudnamutana Subgroup|32364|6|Mentioned|p16|||||||||
21049|Yudnamutana Subgroup|32720|6|Mentioned|p7|||Correlation. Age||||||
21049|Yudnamutana Subgroup|32722|6|Mentioned|Fig.3|||Adelaidean. Stromatolite||||||
21049|Yudnamutana Subgroup|32724|6|Mentioned|Fig.1|||Correlation. Sturtian||||||
21049|Yudnamutana Subgroup|35353|6|Mentioned|Fig.6|||Soil sampling||||||
21049|Yudnamutana Subgroup|36137|5|Briefly described|p3|||||||||
21049|Yudnamutana Subgroup|36833|6|Mentioned|p6|||||||||
21049|Yudnamutana Subgroup|36838|6|Mentioned|p57|||||||||
21049|Yudnamutana Subgroup|37238|6|Mentioned|Table 1|||||||||
21049|Yudnamutana Subgroup|37461|4|Described|p339|||See also Table 5.I||||||
21049|Yudnamutana Subgroup|37932|3|Fully described|p537|||||||||
21049|Yudnamutana Subgroup|38157|6|Mentioned|Table IV|||||||||
21049|Yudnamutana Subgroup|39210|6|Mentioned|Table 4|||||||||
21049|Yudnamutana Subgroup|39344|6|Mentioned|Map legend|Precambrian|Precambrian|Sturtian||||||
21049|Yudnamutana Subgroup|39352|6|Mentioned|Map legend|Precambrian|Precambrian|Sturtian||||||
21049|Yudnamutana Subgroup|40294|6|Mentioned|p41|||||||||
21049|Yudnamutana Subgroup|40911|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
21049|Yudnamutana Subgroup|41401|6|Mentioned|Table 4|||||||||
21049|Yudnamutana Subgroup|41405|6|Mentioned|p125|||||||||
21049|Yudnamutana Subgroup|41526|6|Mentioned|p3|||||||||
21049|Yudnamutana Subgroup|41647|5|Briefly described|p834|||||||||
21049|Yudnamutana Subgroup|41770|6|Mentioned|p237|||||||||
21049|Yudnamutana Subgroup|42215|6|Mentioned|Fig.2 P448|||||||||
21049|Yudnamutana Subgroup|42222|4|Described|p15|||||||||
21049|Yudnamutana Subgroup|42240|6|Mentioned|Fig.2 P165|||||||||
21049|Yudnamutana Subgroup|42272|6|Mentioned|p402|||||||||
21049|Yudnamutana Subgroup|42720|5|Briefly described|map legend|Sturtian||||||||
21049|Yudnamutana Subgroup|43052|5|Briefly described|p183,Table 6.1|||Of the Umberatana Group.||||||11-SEP-07
21049|Yudnamutana Subgroup|43086|6|Mentioned|Appendix, Stop 7|||of Umberatana Group||||||12-JUL-16
21049|Yudnamutana Subgroup|45041|6|Mentioned|p45|||Refers Coats (1964)||||||
21049|Yudnamutana Subgroup|45155|6|Mentioned|p26|||||||||
21049|Yudnamutana Subgroup|46865|6|Mentioned|p50|||||||||
21049|Yudnamutana Subgroup|60718|5|Briefly described|p49 Fig. 2|Adelaidean|Adelaidean|Geological Province: Adelaide Geosyncline.||Of Umberatana Group.|Includes Wilyerpa Formation.|||15-APR-11
21049|Yudnamutana Subgroup|60953|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Glaciomarine diamictite, sandstone, siltstone, conglomerate and ironstone.||||||
21049|Yudnamutana Subgroup|60959|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Of the Umberatana Group.||||||
21049|Yudnamutana Subgroup|61108|5|Briefly described|map legend|Adelaidean|Adelaidean|Glaciomarine diamictite, sandstone, siltstone, conglomerate and ironstone.||||||
21049|Yudnamutana Subgroup|61238|5|Briefly described|p44 Fig. 1|Neoproterozoic|Neoproterozoic|Of the Umberatana Group.||||||11-SEP-07
21049|Yudnamutana Subgroup|61732|5|Briefly described|p28 Fig. 13|Sturtian|Sturtian|Of the Umberatana Group. Includes the Wilyerpa Formation, Appila and Pualco Tillites, and Benda Siltstone.  Geological Province: Adelaide Rift Complex.||||||07-FEB-11
21049|Yudnamutana Subgroup|62085|6|Mentioned|p19 Fig.4|Cryogenian|Cryogenian|Sturtian.||Umberatana Group|||Diamictite, siltstone, quartzite, ironstone.|
21049|Yudnamutana Subgroup|62592|5|Briefly described|p20 Fig.2.4, p50 Table 5.1, pp57-58.|Sturtian|Sturtian|Adelaide Geosyncline. Typo: Yudnamntana SubGroup (Fig.2.4). Colour scheme shown for interpretation of Curnamona seismic sections. Base is clearly defined seismically. Is extremely thick (c.3.5 km) in Flinders Ranges.||Basal unit in Umberatana Group.|Includes Pualco Tillite, Benda Siltstone and Wilyerpa Formation.|Unconformably overlies Burra Group and Skillogalee Dolomite. Is unconformably overlain by Nepouie Subgroup.||08-JUL-13
21049|Yudnamutana Subgroup|62664|6|Mentioned|p138 Fig.2.|Neoproterozoic|Neoproterozoic|||Basal unit in Umberatana Group.|||Tillite, glaciogenic sediments.|
21049|Yudnamutana Subgroup|62724|5|Briefly described|p16, p17 Fig. 4|Sturtian|Sturtian|Of Umberatana Gp. Comprises several facies two of which are Benda Siltst + Pualco Tillite; a section comprising cglm + arkose facies as the Old Boolcoomata Cglm Mbr (Benda Siltst). Galciomarine rocks. Disconformably overlies Burra Gp.||||||07-FEB-11
21049|Yudnamutana Subgroup|62903|5|Briefly described|p729, p730 Fig.1|Sturtian|Sturtian|Adelaide Rift Complex.|||Sturt, Appila, Pualco, Bolla Bollana, and Merirjina (misspelling of Mirinjira) Tillites, Wilyerpa Formation and Lyndhurst Formation.|overlain by Tindelpina Shale Member (Tapley Hill Formation)||
21049|Yudnamutana Subgroup|62962|6|Mentioned|p2284 Fig. 2|Adelaidean|Adelaidean|Geological Province: Mount Painter Province.||||||07-FEB-11
21049|Yudnamutana Subgroup|62993|6|Mentioned|p44|Neoproterozoic|Neoproterozoic||||Includes Benda Siltstone?|||
21049|Yudnamutana Subgroup|63102|5|Briefly described|p8|Sturtian|Sturtian|Geological province: Curnamona Province. Glacial deposits.|||Includes Wilyerpa Formation, Pualco Tillite and Benda Siltstone.|||22-OCT-19
21049|Yudnamutana Subgroup|63458|6|Mentioned|p897 Fig.19. |Cryogenian|Cryogenian|||Unit in Umberatana Group.|Includes Wilyerpa Formation.|||
21049|Yudnamutana Subgroup|63489|5|Briefly described|Map legend|Adelaidean|Adelaidean|Diamictite, siltstone, sandstone, minor carbonate; with the Braemar ironstone facies in the Olary region. New South Wales equivalent is Yancowinna Subgroup.||||||10-SEP-07
21049|Yudnamutana Subgroup|64647|6|Mentioned|p38 Fig. 1|||||||||
21049|Yudnamutana Subgroup|64801|6|Mentioned|p110 Fig.2, p111|Neoproterozoic|Neoproterozoic|Adelaide Rift Complex. Major Sturtian glacial sequence.||Umberatana Group.||||
21049|Yudnamutana Subgroup|64846|5|Briefly described|p198 Fig.3|Cryogenian|Cryogenian|Sturtian glaciation.|658 Ma.|Of the Umberatana Group.|Includes Merinjina Tillite.|||
21049|Yudnamutana Subgroup|65376|6|Mentioned|p92 Fig. 2.82. |Neoproterozoic|Neoproterozoic|||||||
21049|Yudnamutana Subgroup|65493|5|Briefly described|p910, p909 Fig 2|Cryogenian|Cryogenian|Basal Sturtian glacial deposits of the Umberatana Group. Includes Merinjina Tillite. Unconformably overlain by Nepouie Subgroup.||||||
21049|Yudnamutana Subgroup|65921|6|Mentioned|p2 (map legend)|Neoproterozoic|Neoproterozoic|||||||
21049|Yudnamutana Subgroup|65925|5|Briefly described|Appendix 2.||||||||Diamictite; siltstone; pebbly dolomite; orthoquartzite. Glaciomarine.|
21049|Yudnamutana Subgroup|66518|6|Mentioned|p19 Fig.4.|Neoproterozoic|Neoproterozoic|Coombalarnie Platform.||Unit in Umberatana Group.||||
21049|Yudnamutana Subgroup|67180|5|Briefly described|p601 Fig.1, p602 Fig.2|Cryogenian|Cryogenian|Sturtian age.||Unit in Umberatana Group|Includes Merinjina Tillite|Underlies the Nepouie Subgroup.||
21049|Yudnamutana Subgroup|67653|6|Mentioned|p5,11|||Geological province: Curnamona Province.||||||
21049|Yudnamutana Subgroup|67870|5|Briefly described|p9|Neoproterozoic|Neoproterozoic|Adelaide Rift System.||Umberatana Group.|Pualco, Wilyerpa Formations.|||21-JAN-19
21049|Yudnamutana Subgroup|67979|5|Briefly described|p528, p531 Fig.2, p542|Sturtian|Sturtian|Sturtian glacial (Coats and Blissett 1971).||basal succession of Umberatana Group|Includes Merinjina Tillite, Bolla Bollana Formation, Lyndhurst Formation, and Wilyerpa Formation|is overlain by Nepouie Subgroup||
21049|Yudnamutana Subgroup|68067|6|Mentioned|Map legend.|||Areas with higher magnetic response are mapped separately.||||||27-AUG-13
21049|Yudnamutana Subgroup|68068|5|Briefly described|Map legend|Sturtian|Sturtian|Adelaide Geosyncline.||Unit in Umberatana Group.|Includes Fitton Formation and Bolla Bollana Tillite.|||
21049|Yudnamutana Subgroup|68274|6|Mentioned|p12 Fig.1.6, p13|Sturtian|Sturtian|||||||
21049|Yudnamutana Subgroup|68276|6|Mentioned|p68|Neoproterozoic|Neoproterozoic|"The ""Subgroup"" is omitted."||||||
21049|Yudnamutana Subgroup|69019|5|Briefly described|p41-45, p143.|Neoproterozoic|Neoproterozoic|Major sediment thickness changes occur across the Paralana (syndepositional extensional) Fault.|c.658 Ma (U-Pb zircon; Fanning and Link, 2006).|Unit in Umberatana Group.|Includes Fitton Formation, Bolla Bollana Tillite and Wilyerpa Formation, Serle Conglomerate.|||
21049|Yudnamutana Subgroup|69023|5|Briefly described|p51, p64-65, p75, p146, p153-154|Neoproterozoic|Neoproterozoic|Redefined by Preiss et al. (1998). Adelaidean. Includes all Sturtian glaciogenic sediments in this area. Major sediment thickness differences either side of the Paralana Fault.||Unit in Umberatana Group.|Includes Fitton Formation, Bolla Bollana Tillite and Lyndhurst Formation.|Is intruded by Mudnawatana Tonalite.|Metasediments.|
21049|Yudnamutana Subgroup|70031|5|Briefly described|p245|Cryogenian|Cryogenian|Adelaide Geosyncline. Associated with Sturtian glaciation.||Unit of Umberatana Group.|Incldues Wilyerpa Formation, Benda Siltstone, Pualco Tillite and Holowilena Ironstone.|Overlain by Tindelpina Shale Member/Tapley Hill Formation/Nepouie Subgroup.||
21049|Yudnamutana Subgroup|70323|4|Described|p211-213,219-220|Cryogenian|Cryogenian|Central Flinders Ranges, Adelaide Geosyncline. Associated with Sturtian glaciation. Deposited in the NW-SE-oriented marine rift complex of the Baratta Trough.|c. 660 Ma|Unit of Umberatana Group.|Includes Wilyerpa Formation, Holowilena Ironstone and Pualco Tillite.|Overlain by Nepouie Subgroup/Tapley Hill Formation. Underlain by Burra Group.||
21049|Yudnamutana Subgroup|70384|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Adelaide Geosyncline. Age shown more specifically as Sturtian [Cryogenian].||Umberatana Group.|Includes Fitton, Lyndhurst Formations; Merinjina, Bolla Bollana Tillites.|Unconformably overlies Bungarider Subgroup (Burra Group). Is overlain unconformably by Nepouie Subgroup.||21-JAN-19
21049|Yudnamutana Subgroup|70405|6|Mentioned|p14 figure 6, p51 table 4 |Neoproterozoic|Neoproterozoic|Sturtian glacial sediments.|||Includes Wilyerpa Formation, Benda Siltstone, Old Boolcoomata Conglomerate Member, Benda Siltstone, Pualco Tillite|||
21049|Yudnamutana Subgroup|70657|5|Briefly described|p9 Fig.3|Neoproterozoic|Neoproterozoic||||Includes Wilyerpa Formation, Benda Siltstone, Pualco Tillite.||Sturtian glacials.|
21049|Yudnamutana Subgroup|70658|6|Mentioned|p14|Neoproterozoic|Neoproterozoic||||Sturtian glacials, Wilyerpa Formation, Benda Siltstone, Pualco Tillite.|||
21049|Yudnamutana Subgroup|70819|6|Mentioned|p11, 13, 29|Neoproterozoic|Neoproterozoic|Clare Valley. Confusingly, Fig.4 on p13 clearly shows this Subgroup as part of the Burra Group.||Umberatana Group.|Appila Tillite, Wilyerpa Formation.|Overlies Belair Subgroup (Burra Group). Is overlain by Nepouie Subgroup.||
21049|Yudnamutana Subgroup|72613|6|Mentioned|p2|Cryogenian|Cryogenian|Represents the entire Sturtian glacial succession in the Adelaide Fold belt.||Umberatana Group|Includes Merinjina Tillite.|Conformably overlain by the Tapley Hill Formation.|Diamictite and ice-rafted debris.|
21049|Yudnamutana Subgroup|73188|6|Mentioned|p316|Neoproterozoic|Neoproterozoic|Mount Lofty Ranges.||Umberatana Group|Sturt Tillite|||
21049|Yudnamutana Subgroup|73236|6|Mentioned|p36, p38|Cryogenian|Cryogenian|Marine sedimentary rocks.||Umberatana Group, Heysen Supergroup|Sturt Tillite|Overlain by Tapley Hill Formation (Nepouie Subgroup).||
21049|Yudnamutana Subgroup|73251|6|Mentioned|p36|Neoproterozoic|Neoproterozoic|Coombalarnie Platform.||Umberatana Group|||Metasediments.|
21049|Yudnamutana Subgroup|74367|5|Briefly described|p7 Fig.6, p8, p18, p21-22|Cryogenian|Cryogenian|Minimum age of 663.03+/-0.11 Ma constrained by the Wilyerpa Formation (Cox et al., 2018).||Umberatana Group|Bolla Bollana Tillite, Appila Tillite, Wilyerpa Formation||Glacial sedimentary rocks.|
21068|Yundi Sandy Loam|38290|5|Briefly described|p61|||||||||
21070|Yuruga Formation|22643|5|Briefly described|fig3p187, fig6|Middle Cambrian|Middle Cambrian|||||||
21070|Yuruga Formation|22755|6|Mentioned|p555||Cambrian|||||||
21070|Yuruga Formation|22766|5|Briefly described|Fig.2 p561, p563|Middle Cambrian|Middle Cambrian|||||||
21070|Yuruga Formation|23981|5|Briefly described|p8-9 Fig. 4, p45 Fig. 15|Cambrian|Cambrian|Mainly of red-brown, x-bedded, fine-grained, feldspathic sandstone and siltstone, with dessication cracks, mudchip breccias and arthropod tracks at several levels. Overlies Coobowie Formation. Thickness in Stansbury town: 548m. Geol. P: Stansbury Basin.||||||04-FEB-08
21070|Yuruga Formation|24465|5|Briefly described|p345 Fig.2|Cambrian|Cambrian|Geological Province: Stansbury Basin.||||||19-JAN-05
21070|Yuruga Formation|35255|6|Mentioned|Fig.8|||||||||
21070|Yuruga Formation|36244|6|Mentioned|p2|||Refers Thomson et al.1976.||||||
21070|Yuruga Formation|38873|4|Described|p17|||||||||
21070|Yuruga Formation|40856|6|Mentioned|Fig.23.6|||||||||
21070|Yuruga Formation|42222|6|Mentioned|Table 1 P4|||||||||
21070|Yuruga Formation|42225|4|Described|p226|||||||||
21070|Yuruga Formation|42269|6|Mentioned|Fig.1 P335|||||||||
21070|Yuruga Formation|43052|5|Briefly described|Table 2.1|||||||||
21070|Yuruga Formation|43053|5|Briefly described|Map Legend|Cambrian|Cambrian|Shallow marine to terrestrial redbeds, peritidal to marine limestone.||||||25-MAY-05
21070|Yuruga Formation|43258|5|Briefly described|Map Legend||Cambrian|||||||
21070|Yuruga Formation|43298|6|Mentioned|Map Legend||Cambrian|||||||
21070|Yuruga Formation|44133|5|Briefly described|p18, p4 Fig. 7.2, 6|Middle Paleozoic|Early Paleozoic|Geological Province: Stansbury Basin. Maximum Thickness: 548m.||||||07-NOV-08
21070|Yuruga Formation|60953|5|Briefly described|Map Legend|Cambrian|Cambrian|Geological Province: Spencer Shelf.||||||
21070|Yuruga Formation|60958|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Red-brown, arkosic sandstone, sandy siltstone and conglomerate. Massive to cross bedded. Geological Province: Stansbury Basin.||||||14-APR-05
21070|Yuruga Formation|61108|5|Briefly described|map legend|Cambrian|Cambrian|Shallow marine to terrestrial redbeds; peritidal to marine limestone. Geological Province: Spencer Shelf.||||||
21070|Yuruga Formation|61121|5|Briefly described|Map legend|Middle Cambrian|Middle Cambrian|Red-brown, arkosic sandstone, sandy siltstone and conglomerate; massive to cross-bedded; trilobite tracks. Geological Province: Stansbury Basin.||||||06-JUN-05
21070|Yuruga Formation|64282|5|Briefly described|Map legend|Early Cambrian|Early Cambrian|Geological Province: Stansbury Basin. Red-brown arkosic sandstone, sandy siltstone and conglomerate. Fluvio-lacustrine to shoreface; trilobite tracks.||||||24-JUL-08
21070|Yuruga Formation|65375|4|Described|p27 Fig.5, pp31-32, p34.|Middle Cambrian|Middle Cambrian|Up to 548m thick. Trace fossils and trilobite tracks occur. Youngest Cambrian deposit on Yorke Peninsula.||||Overlies Coobowie Limestone. Is unconformably overlain by Cape Jervis Formation.|Red-brown fluvial sandstone, generally haematitic and arkosic; conglomerate and breccia; minor thin siltstone layers.|
21070|Yuruga Formation|65892|5|Briefly described|p9 Fig.4. |Middle Cambrian|Middle Cambrian|Yorke Peninsula.||||Overlies Coobowie Limestone. Correlative of Pantapinna Sandstone.||
21070|Yuruga Formation|67536|6|Mentioned|Map Legend||||||||Shallow marine to terrestrial redbeds.|01-APR-14
21070|Yuruga Formation|68735|6|Mentioned|p233 Fig.2, p235 Fig.3|Middle Cambrian|Middle Cambrian|Stansbury Basin.||||||
21070|Yuruga Formation|68993|6|Mentioned|p544 Fig.1|Middle Cambrian|Middle Cambrian|Yorke Peninsula.||||||
21070|Yuruga Formation|73092|6|Mentioned|p2|Cambrian|Neoproterozoic|||||||
21070|Yuruga Formation|73107|5|Briefly described|Map legend.|Early Cambrian|Early Cambrian|Stansbury Basin.|||||Red-brown, arkosic sandstone, sandy siltstone and conglomerate. Fluvial lacustrine to shoreface. Trilobite tracks. Subsurface only.|
21070|Yuruga Formation|73188|6|Mentioned|p343|Cambrian|Cambrian||||||[Redbeds?].|
