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Lake Woorong. First partial surrender report, for the period 8/6/2012 to 7/6/2015.
An area centred about 80 km south-west of Coober Pedy is being explored for possible economic buried coal seams in Permian strata and for economic iron ore deposits or massive sulphide base metal mineralisation (copper, nickel) that may have formed...-
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Bulgunnia. Progress reports and final report to licence full surrender, for the period 22/5/1978 to 10/8/1981.
The base metal and uranium potential of a concealed Proterozoic basement high near Bulgunnia Homestead was evaluated using geological and hydrogeochemical reconnaissance and regional geophysical interpretation approaches. Seismic, ground magnetic and...-
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Carnding. Annual reports and final report to licence full surrender, for the period 18/1/2006 to 22/2/2012.
Three separate small sub-blocks forming a licence in the Tarcoola district have been explored for possible economic buried Tertiary sandstone-hosted uranium mineralisation and for any other metallic mineralisation that may have formed in underlying...-
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Published: 29 Feb 1912
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RB 2020/00012 Gawler Craton Airborne Geophysical Survey Region 8A, Coober Pedy West – Enhanced geophysical imagery and magnetic source depth models
This report presents the results of a study jointly conducted by the Geological Survey of South Australia and CSIRO Mineral Resources which aimed to enhance the expression of geological structure in geophysical images and to derive depth to magnetic...-
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Published: 01 Apr 2020
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Ingomar Station and Phar Lap Outstation (part of Ingomar JV Project). Joint annual plus separate annual and final reports to licences' expiry/full surrender, for the period 13/6/2002 to 23/7/2007.
Work done on two licences covering inferred Challenger - type vein gold or Olympic Dam / Prominent Hill style IOCG mineralisation - prospective ground that is situated approximately 70 km to the south and south-east of Coober Pedy has been confined to...-
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Published: 22 Aug 1907
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ExpNotes GILES: Explanatory Notes GILES, SH 53-01.
Concealed basement on GILES comprises ?Archaean to Palaeoproterozoic metamorphic rocks belonging to the Nawa Subdomain of the Gawler Craton. These are intruded by Mesoproterozoic Hiltaba Suite granitic bodies and Mesoproterozoic or Neoproterozoic...-
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ExpNotes BARTON: Explanatory Notes BARTON, SH 53-09.
Shallow Precambrian crystalline basement underlies the greater part of the BARTON 1:250 000 map area. Thicker Neoproterozoic, Cambrian and Carboniferous Permian sediments occur in the northwest, with the southern margin bounded by the Karari Fault...-
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