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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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PACE 2020 Discovery Drilling 2012 : Year 7 Drilling Partnership no. DPY7-01 - South Australia Ludi Mining Pty Ltd, Coward Springs area gravity/magnetic anomaly IOCG targets. Drilling project interim report and final report.
South Australia Ludi Mining Pty Ltd (“SALM”) acquired Exploration Licence 4619 “Coward Springs” to explore for large Mesoproterozoic copper/gold/uranium deposits analogous to Olympic Dam, which is located approximately 120 km to the south. The licence...-
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RB 2007/00006 The geology and mineral potential of the PORT AUGUSTA [mapsheet] area, eastern Gawler Craton.
The PORT AUGUSTA 1:250,000 mapsheet area covers the north-eastern part of the Eyre Peninsula, the northern Spencer Gulf and the south-western Flinders Ranges, and extends from latitude 32°00'S to 33°00'S and longitude 136°30'S to 138°00'S. The main...-
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Published: 01 Apr 2007
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RB 2014/00006 Geology of the Cultana 1:100 000 map sheet (6432).
The revised digital geology map of the Cultana 1:100 000 map sheet and accompanying geological descriptions in this report are the first components of the 2nd edition PORT AUGUSTA 1:250 000 map sheet to be completed. The subject map sheet occupies the...-
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Published: 01 Jan 2014
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Cultana, South Australia. Sheet 6432, International Index. 1:100 000 Geological Series digital map.
Cultana is located on parts of the north-eastern Eyre Peninsula, northern Spencer Gulf and south-western Flinders Ranges, and is underlain by rocks of the Mesoarchaean-Mesoproterozoic Gawler Craton, the Neoproterozoic Adelaide Geosyncline, Torrens...-
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Published: 29 Apr 2014
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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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