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Willouran Ranges Stratiform Copper Project. Quarterly reports and annual reports to licence expiry/full surrender, for the period 22/12/1976 to 21/12/1978.
Detailed geological mapping, rock and soil sample geochemistry, sedimentary petrology, and rotary percussion and diamond drilling were undertaken in the Willouran Ranges, south-west of Marree, to explore for stratiform copper mineralisation,...-
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Data release - as updated : Castle Rock. Annual reports to licence full surrender, for the period 17/3/2009 to 14/1/2016.
Exploration for possible economic concealed Beltana mine type stratabound lead-zinc-(silver) mineralisation, and for other diapiric and associated basic igneous intrusion - related base metal and/or gold occurrences, was carried out over a small area...-
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Published: 20 Jan 1916
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RB 2012/00004 MARREE, South Australia, [geological map] sheet SH54-5. South Australia. Geological Survey. 1:250 000 Series - Explanatory Notes.
The MARREE mapsheet area includes the south-western portion of the Strzelecki Desert plus parts of the Tirari Desert, north-western Flinders Ranges and north-eastern Willouran Ranges, between latitudes 29 to 30 degrees S and longitudes 138 to 139...-
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Published: 01 Apr 2012
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Mount Denison (part of the BHP Billiton - Rio Tinto - Phelps Dodge' Peake and Denison Joint Venture Project). First partial surrender report, for the period 12/7/1993 to 16/9/2003.
Exploration carried out over the northern Peake and Denison Ranges since 1993 has targeted possible large-scale Proterozoic iron oxide associated copper-gold (IOCG) deposits considered to have formed in stratigraphic/structural settings similar to...-
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ExpNotes MARREE: Explanatory Notes MARREE
A new generation, second edition MARREE 1:250 000 scale geological map and its explanatory notes have been published. These documents represent the conclusion of the Geological Survey of South Australia's latest geological mapping program (1993 to...-
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ExpNotes PARACHILNA (v2): Explanatory Notes PARACHILNA (second edition, 1999)
The PARACHILNA map area (31 to 32°S, 138 to 139.5°E) occupies the central Flinders Ranges which are made up of folded, mostly marine sedimentary Neoproterozoic and Cambrian rocks of the Adelaide Geosyncline, and adjoining plains underlain by Cainozoic...-
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