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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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Geochronological synthesis of southern Australia - Part 1 The Curnamona Province, and Part 2 The Gawler Craton (SADME Data Package.).
The review reports in this data package present a synthesis of geochronological information for southern Australia, i.e. South Australia and geologically associated areas in New South Wales and Victoria. The data given represent the outcomes of much...-
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Published: 19 Sep 1997
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Data release - as updated [made at SA Director of Mines' discretion] : Prospect Hill. Annual reports for the period 25/7/2006 to 24/7/2018.
Continued evaluation of possible economic primary tin oxide mineralisation at three known separate occurrences in the Prospect Hill area, lying 20 km north-west of Moolawatana Homestead, has focussed on the untested zone immediately below the known...-
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Unlocking South Australia's Mineral and Energy Potential - A Plan for Accelerating Exploration. PACE Copper Discovery Drilling (drilling partnerships with DSD and industry) : Year 9 partnership no. DPY9-12 - Prospect Hill. Drilling project final report.
Prospect Hill is South Australia’s best known tin occurrence, with an inferred resource of 172,800 t @ 1.15% Sn to 50 vertical metres estimated at the South Ridge prospect. Significant base metals are associated with the tin, and the mineralisation is...-
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Published: 30 May 1917
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CALLABONNA 1:250 000 geological map released.
There is no abstract created for this record-
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PACE Theme 2 (drilling partnerships with PIRSA and industry): Year 4 partnership DPY4-42, Prospect Hill Project area Proterozoic tin and base metals mineral prospects. Project final report.
The Prospect Hill area, situated at the extreme northern end of the Flinders Ranges, is extensively tin-mineralised, with fine-grained polymetallic, probable porphyry-style cassiterite veins dispersed in Mesoproterozoic volcanic and tuffaceous...-
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