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...

The surrendered two remnant portions EL 5725 Mount Deception formerly were part of a much larger multi-tenement package which is currently still being explored by Perilya, primarily looking for economic stratabound zinc silicate mineralisation similar...

Copper Range has targeted several different styles of base metal mineralisation within the Chace Range district. Initially its focus was on sediment (sandstone)- hosted copper deposits, with exploration being confined to reconnaissance field visits to...

An intensely faulted and folded metasedimentary area centred ~50 km east-northeast of Blinman, where extensive hydrothermal alteration is evident in the Neoproterozoic bedrock, and where considerable past small-scale surface mining activity has...

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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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...