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RB 37/00039 Report on the Copper King ochre deposits (near Beltana).
The Copper King orebody, located approximately 10 miles north-northeast of Beltana township, is a massive deposit of iron carbonate, the upper portion of which has been altered by oxidation and hydration to oxides of iron. The deposit was worked...-
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Published: 09 Mar 1954
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Data release [made at SA Director of Mines' discretion] : Beltana / Copley. Annual reports to licence expiry/renewal, for the period 15/4/1994 to 24/6/2003.
A portion of the central Flinders Ranges covering the Beltana Diapir and its surrounds has been taken up mainly to explore for possible economic buried hydrothermal replacement type or epigenetic stratabound base metal mineralisation, with magnesite...-
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Published: 23 Dec 1914
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RB 2014/00002 Carbonate hosted Pb-Zn-Ag deposits. exploration using light hydrocarbons as pathfinders.
Surveys recently conducted in England, Ireland and Australia have shown that there are major spatial variations in the 'light' [molecular weight] hydrocarbon gas content of rocks which are closely related to the presence of underlying mineralisation....-
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Published: 01 Jul 1995
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Puttapa. Progress reports for the period 11/1/1969 to 15/7/1970.
Ongoing base metal exploration to look for further analogues to the Beltana willemite discovery, carried out over an area located east of the Puttapa Rail Siding, has consisted of semi-detailed 1:4800 scale geological mapping and geochemical stream...-
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Beltana. Progress reports to licence expiry/renewal, for the period 14/12/1973 to 13/12/1975.
A geological and geochemical appraisal made of various mines and prospects in the Beltana area has sugggested that only those situated nearest the Nuccaleena Diapir are the most likely to yield drilling success in the search for significant extensions...-
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Report on Beltana concessions, Special Mining Leases 113, 136 and 142, SA.
An area surrounding Beltana in the Flinders Ranges, which is known to contain low level base metal mineralised Adelaidean and Cambrian sedimentary rocks and diapiric intrusive structures, has been prospected by a combination of photogeological studies...-
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