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South Australian geological field [guides] and excursion guides.
There is no abstract created for this record-
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Wirrealpa. Progress, partial surrender and final reports to licence surrender for the period 13/11/1978 to 26/2/1988.
Economic deposits of Mississippi Valley type stratabound lead-zinc mineralisation within in Cambrian limestones were the targets of exploration undertaken on and near the Wirrealpa Diapir. A preliminary field reconnaissance had shown that surface...-
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Mount Uro. Progress, partial surrender [and ?final] reports to licence surrender for the period 29/4/1984 to 26/2/1987.
Adelaidean and Cambrian calcareous clastic rocks of the Angepena region were investigated for possible economic epigenetic base and precious metal mineralisation that may be related to syn-depositional faulting, as well as for stratiform and...-
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Jubilee Hill. Annual reports to licence expiry/full surrender, for the period 22/4/1998 to 21/4/2003.
Exploration of a small area of Neoproterozoic and Cambrian fold belt strata in the Jubilee Hill - Mount Roebuck area, located 45 km east-northeast of Blinman, was aimed at finding possible economic base and precious metal mineralisation associated...-
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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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Central Flinders Ranges, part PARACHILNA [mapsheet area] regional geology 3D Model (3D pdf version 1)
Upper crustal strata forming 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...-
Model
- ZIP,
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Central Flinders Ranges, part PARACHILNA [mapsheet area] regional geology 3D Model (GOCAD version 1).
Upper crustal strata forming 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...-
Model
- ZIP,
