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RB 91/00041 Geology of the KINGOONYA 1:250 000 map sheet area.
Extensive field geological mapping, augmented by petrological and geochemical studies, reinterpretation of company drilling and water-bore logs and a nine-hole drilling programme has detailed the geology of the KINGOONYA area. The stratigraphy spans...-
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Published: 01 Apr 1991
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RB 93/00010 Explanatory Notes for the WARRINA 1:250 000 geological map.
The oldest rocks on WARRINA outcrop in the Peake and Denison Inliers, which comprise the Davenport and Denison Ranges and small inliers to the east. Basement in this area consists of Palaeoproterozoic metamorphic rocks which were intruded by...-
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Published: 01 Jun 1994
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RB 90/00014 Explanatory Notes for the TALLARINGA 1:250 000 geological map.
There is no abstract created for this record-
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Published: 01 Mar 1991
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Tallaringa and Mount Igy (the Tallaringa JV Project). Joint annual reports to licences' joint full surrender, for the period 18/1/2009 to 6/2/2015.
During the 2009-2010 project joint reporting year, the following activities occurred: - the conduct of an Aboriginal heritage work area clearance survey in the northern part of EL 3485 Tallaringa by the Antakarinja Land Management Council Native...-
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Wilkinson Lakes East. Annual reports plus final report to licence full surrender, for the period 3/5/2010 to 6/2/2015.
An area centred ~150 km west of Coober Pedy, that is located mostly north-west of and that also has a small part lying immediately south-east of the Karari Fault, a major crustal structure which has controlled deposition at the southern limit of the...-
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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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RB 74/00177 Progress report on the geology of the COOBER PEDY 1:250 000 sheet area (pre-Quaternary).
The Coober Pedy 1:250 000 sheet area (COOBER PEDY) is bounded by latitudes 29°S and 30°S and by longitudes 133°E and 135°E in the arid north of South Australia. The only town is the opal mining town of Coober Pedy on the northeastern margin of the...-
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Published: 01 Jan 1974
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RB 2006/00001 Guide to the sedimentary cover of the central Gawler Craton, South Australia
The central Gawler Craton is blanketed by thin sedimentary cover that ranges in age from Neoproterozoic to Quaternary. Locally, though, such cover can reach a maximum of ~500 m thickness in Permian glacial valleys or rift structures. This guide...-
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Published: 01 Jan 2006
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RB 2014/00005 WINTINNA, South Australia, [geological map] sheet SG53-14. South Australia. Geological Survey. 1:250 000 Series - Explanatory Notes.
The WINTINNA 1:250 000 mapsheet area lies between latitudes 27° to 28° South and longitudes 133°30’ to 135°00’ East. This ~16 400 square km area includes the Marla and Cadney Park settlements, and is crossed by the Stuart Highway and Adelaide to...-
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Published: 01 Mar 2015
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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
- PDF,
- ZIP
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RB 2010/00002 GOMA basement drilling program, northern Gawler Craton.
The GOMA basement drilling program was named after the Gawler-Officer-Musgrave-Amadeus deep seismic reflection survey line, that was completed in 2008 by Geoscience Australia (GA) as part of its Onshore Energy Security Program. Funding for the seismic...-
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Published: 01 Feb 2010
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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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ExpNotes COOBER PEDY: Explanatory Notes COOBER PEDY, SH 53-06.
There is no abstract created for this record.-
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RB 2023/00043 Remapping the paleovalley systems of the central-western Gawler Craton, South Australia.
The Geological Survey of South Australia’s (GSSA) Gawler Challenge Phase 2: next generation mineral systems mapping (GP2) program allowed the authors of this report to revisits some ground-breaking landscape evolution studies with new geophysical data...-
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Published: 01 Dec 2023
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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 WINTINNA: Explanatory Notes WINTINNA, SG 53-14.
A new generation, first edition WINTINNA 1:250 000 scale geological map and explanatory notes have been published. These documents represent the conclusion of the Geological Survey of South Australia's geological mapping program undertaken in the...-
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ExpNotes WARRINA: Explanatory Notes WARRINA, SH 53-03.
The Peake and Denison Inliers (comprising the Davenport Range, Denison Range and small basement inliers to the east) form the dominant geological structure on WARRINA. The Inliers include outcrops of Palaeoproterozoic metamorphic basement which is...-
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ExpNotes KINGOONYA: Explanatory Notes KINGOONYA, SH 53-11.
There is no abstract created for this record.-
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ExpNotes TALLARINGA: Explanatory Notes TALLARINGA, SH 53-05.
There is no abstract created for this record.-
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Cudyea. Annual reports and final report to licence expiry/full surrender, for the period 2/1/2007 to 1/1/2011.
Mineral exploration conducted in an area centred approximately 125 km west of Tarcoola has addressed targets including possible Challenger type metamorphic gold mineralisation or Olympic Dam type epithermal IOCG mineralisation, and also less deeply...-
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Published: 21 Mar 2011
