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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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RB 89/00023 Excursion guide for Willyama Supergroup and related rocks, Olary District, SA.
This 4-day field trip demonstrates :- Willyama Complex (basement) stratigraphy,- deformation and metamorphic style of the Olarian, Orogeny (including possible recumbent folds), - large blocks of granite and migmatite, up to 800 metres, long, within...-
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Published: 01 Apr 1989
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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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Walparuta. Annual reports and final report to licence expiry/full surrender, for the period 21/6/2010 to 20/6/2019.
A small area centred ~30 km west of Olary has been explored for possible economic buried primary stratiform base metal sulphide mineralisation, vein barite mineralisation and also for epithermal copper-gold deposits that may have formed in...-
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Luxemburg Well. Progress and final reports for the period 4/11/83 to 3/11/84.
Diamond drillcore obtained from the Luxemburg mine area, which was drilled by Sundowner Minerals Pty Ltd in 1969-70, was assayed and identified as consisting of altered pyroxenite, altered granitoids (adamellite, granodiorite, tonalite), and altered...-
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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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