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Data release - as updated [made at SA Director of Mines' discretion] : Red Range (part of the Copley Project). Annual reports for the period 8/10/2007 to 7/10/2018.
A small area located 45 km north-east of Leigh Creek, which covers the sites of numerous small historic diggings made by prospectors searching for copper and lead-zinc-silver mineralisation, is now being explored afresh for possible economic...-
Document
Published: 17 Nov 1917
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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...-
Document
Published: 01 Apr 2012
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Angepena. Progress and technical reports to licence expiry/renewal for the period 18/12/1967 to 17/12/1969.
Geological and geochemical investigations undertaken in the vicinity of the historic Mucatoona copper occurrence indicate that the Angepena ?diapiric breccia zones have no potential for hosting economic mineralisation. There is only a marginal...-
Document
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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...-
Document
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Northern Flinders Ranges, part COPLEY [mapsheet area] regional geology 3D Model (3D pdf version 1)
The northern to central Flinders Ranges area comprise uplifted and eroded remnants of openly folded sedimentary rocks that were deposited in an intra-continental arm of the Neoproterozoic to Early Cambrian Adelaide Geosyncline. Deposition was...-
Model
- ZIP,
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Northern Flinders Ranges, part COPLEY [mapsheet area] regional geology 3D Model (GOCAD version 1).
The northern to central Flinders Ranges area comprise uplifted and eroded remnants of openly folded sedimentary rocks that were deposited in an intra-continental arm of the Neoproterozoic to Early Cambrian Adelaide Geosyncline. Deposition was...-
Model
- ZIP,
