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Data release - as updated [made at SA Director of Mines' discretion] : Wild Horse Plain. Annual reports for the period 8/7/2005 to 23/2/2019, plus partial surrender reports to 23/2/2021.
An upland area located approximately 100 km south-west of Whyalla on the eastern Eyre Peninsula, and with its eastern boundary running parallel to the coast at a distance of 15 km from Cowell and Franklin Harbour, is being explored for uranium,...-
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Published: 11 Jan 1921
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RB 2001/00006 Reconnaissance sampling of basement rocks of the Gawler Craton, South Australia, for dimension stone.
Eighty-five sites of crystalline basement rocks on the Gawler Craton were inspected to determine which lithological or stratigraphical units have potential for use as dimension stone. The Gawler Craton contains a variety of rock types including...-
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Published: 01 Oct 2000
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RB 2012/00019 Geochemistry of pre-1570 Ma mafic magmatism within southern Australia: implications for possible tectonic settings and timing of major mineralisation events in South Australia.
Geochemical and isotopic data from mantle-derived mafic rocks provide important constraints on our understanding of the composition and evolution of the lithosphere through time. Since the lithosphere is sensitive to tectonic processes such as...-
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Published: 01 Dec 2012
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ExpNotes LINCOLN: Explanatory Notes LINCOLN
The LINCOLN 1:250,000 scale regional geological map area covers southern Eyre Peninsula and includes numerous islands lying off its eastern, southern and western coasts. The region encompasses a complex geological history and contains a variety of...-
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RB 2016/00026 Stratigraphy and geochemistry of the 1745–1700 Ma Peter Pan Supersuite.
During the period 1745–1700 Ma, felsic and mafic rocks were intruded throughout the Gawler Craton, broadly coeval with the 1740–1690 Ma Kimban Orogeny. These rocks were previously considered part of the Lincoln Complex, a stratigraphic term defined by...-
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Published: 01 Mar 2017
