ABMINGA lies on the eastern edge of the Musgrave Block, which consists of Early to Middle Proterozoic gneisses and granites, intruded by dolerite dykes. A small area of folded and faulted Adelaidean and Cambrian sediments lies in the SW corner....

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Two major palaeodrainage systems of Tertiary age, with watersheds of up to 35 000 square km and channel lengths of 200-250 km, have been recognised and delineated using LANDSAT imagery, during 1:250 000 scale geological mapping in western South...

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During field mapping on the WINTINNA and MURLOOCOPPIE 1:250,000 sheet areas, the common occurrence of massive "grey-billy" silcretes containing pebbles of (older) silcrete was noted. More recent work on the DALHOUSIE 1:250,000 sheet has revealed that...

Two separate licence areas centred approximately 50 km north of Coober Pedy have been explored for possible economic roll-front style sedimentary uranium mineralisation that may have formed within Palaeozoic and younger cover, and for Olympic Dam type...

The WINTINNA 1:250 000 mapsheet area lies between latitudes 27° to 28° South and longitudes 133°30’ to 135°00’ East. This ~16 400 square km area includes the Marla and Cadney Park settlements, and is crossed by the Stuart Highway and Adelaide to...

There is no abstract created for this record

There is no abstract created for this record

There is no abstract created for this record

A new generation, first edition WINTINNA 1:250 000 scale geological map and explanatory notes have been published. These documents represent the conclusion of the Geological Survey of South Australia's geological mapping program undertaken in the...

The Peake and Denison Inliers (comprising the Davenport Range, Denison Range and small basement inliers to the east) form the dominant geological structure on WARRINA. The Inliers include outcrops of Palaeoproterozoic metamorphic basement which is...