The deformed metasediments of the South Australian Willyama Inliers (in the southern Curnamona geological province) preserve petrologic evidence of a complex and protracted metamorphic history. To assist with unravelling this history, there currently...

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...

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...

Concealed basement on GILES comprises ?Archaean to Palaeoproterozoic metamorphic rocks belonging to the Nawa Subdomain of the Gawler Craton. These are intruded by Mesoproterozoic Hiltaba Suite granitic bodies and Mesoproterozoic or Neoproterozoic...

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The geology of South Australia represents over 150 years of geological investigations in South Australia. It is designed to provide the reader with a comprehensive regional account of the products of sedimentation, deformation, metamorphism and...

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The LINCOLN 1:250,000 scale regional geological map area covers southern Eyre Peninsula and includes numerous islands lying off its eastern, southern and western coasts. The region encompasses a complex geological history and contains a variety of...

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Proterozoic basement outcrops consist of syn and post- Kimban Orogeny granitoids, volcanics and basic dykes. Their rock type geochronology, field relationships and regional correlation are reported. Previous economic mineral investigations, plus...

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The STRZELECKI 1:250 000 map area lies adjacent to the NSW border in the centre of the Strzelecki Desert, and covers some of the main hydrocarbon producing areas in SA around Moomba. Most of these oil and gas fields are located in the northern half of...

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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...