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RB 98/00003 Review of the Proterozoic geology and mineral potential of the Curnamona Province in South Australia.
The Curnamona Province is exposed in the Willyama, Mt Painter and Mt Babbage Inliers, but much is obscured by younger sedimentary cover. It comprises a late Palaeoproterozoic metasedimentary and metavolcanic succession (Willyama Supergroup) with some...-
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Published: 02 Feb 1998
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Morialpa. Data release made in lieu of submitting a first partial surrender report : progress reports and annual reports for the period 16/12/1995 to 8/8/2003.
Initial exploration for stratiform Cu-Au mineralisation hosted within Adelaidean sediments in the Morialpa area, 40 km north- west of Olary, comprised soil, stream sediment, rock chip and ironstone lag geochemical sampling, and 1:10,000 scale...-
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Published: 29 Aug 1903
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RB 2002/00027 Mafic rocks of the Mingary 1:100 000 map area - A review.
The Mingary 1:100 000 map area in the north-east of the state covers part of the Curnamona Province. Five suites of basic intrusives have been identified in the area. The most widespread is a series of amphibole-bearing sills which, having an...-
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Published: 01 Jan 2003
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RB 2009/00001 Explanatory Notes for [the] CALLABONNA 1:250 000 Geological Map, sheet SH 54-6.
The CALLABONNA map area includes the southern end of the Strzelecki Desert and the north- eastern Flinders Ranges, between latitudes 29° to 30° S and longitudes 139° 30' to 141° E. Cameron Corner adjoins New South Wales and Queensland in the...-
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Published: 01 Oct 2009
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Radium Hill. Progress reports to licence expiry/full surrender for the period 29/6/1972 to 28/6/1973.
Exploration for possible economic uranium and/or base metal mineralisation in the Radium Hill district consisted of a consultants' review of the exploration potential of the area based on data from existing mines and prospects, plus the conduct of a...-
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Published: 25 Jul 1973
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Manna Hill. Progress reports to licence expiry/renewal, for the period 8/10/1970 to 7/10/1971.
Exploration for possible economic base metal sulphides hosted within a 10 square mile block of Carpentarian basement schists and gneiss, or within adjoining younger Adelaidean metasedimentary cover rocks, in an area located just north and west of...-
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