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RB 92/00037 Review of mineral exploration, KINGOONYA 1:250 000 map area.
This report was prepared as a summary of all open file mineral exploration data from the KINGOONYA 1:250000 mapsheet area that are held in the SADME records management Envelope system. The aim of the holdings review was to describe past exploration,...-
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Published: 29 Nov 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 97/00008 South Australian Steel and Energy Project. Coober Pedy iron ore investigation. Regional bedrock drilling 1995.
Following the acquisition and interpretation of 435 line km of ground magnetic surveys over selected aeromagnetic anomalies within regions of high magnetic relief on the northern Gawler Craton, 121 reverse circulation holes totalling 8609.25 m were...-
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Published: 01 Jan 1997
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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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ExpNotes WINTINNA: Explanatory Notes WINTINNA
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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Phar Lap Outstation. First partial surrender report for the period 27/8/2007 to 26/8/2010.
An area located at the south-eastern end of the Lake Phillipson Trough in the Arckaringa Basin has been taken up primarily to investigate potential palaeochannels containing lignites or pyritic sands of both Permian and Mesozoic age, which it is...-
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Published: 13 Dec 1910
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Data release - as updated : Phar Lap Outstation. Annual reports plus final report to licence expiry/full surrender, for the period 27/8/2007 to 26/8/2017.
An area centred ~85 km south-southeast of Coober Pedy, at the southern margin of the Lake Phillipson Trough, a long active tectonic feature now occupied by deep sedimentary fill, was taken up by a wholly-owned subsidiary to Monax Mining Ltd primarily...-
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Published: 24 May 1917
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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
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ExpNotes COOBER PEDY: Explanatory Notes COOBER PEDY
There is no abstract created for this record-
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ExpNotes KINGOONYA: Explanatory Notes KINGOONYA
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ExpNotes TALLARINGA: Explanatory Notes TALLARINGA
There is no abstract created for this record-
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ExpNotes WARRINA: Explanatory Notes WARRINA
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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