An area located on and closely marginal to the Denison Inlier of the Proterozoic Peake and Denison Ranges, approximately 80 km south-east of Oodnadatta, was explored for possible roll-front style sedimentary uranium deposits that may have formed...

A small licence area taken up approximately 130 km north of Marla, near the SA/NT state border, is being explored for possible economic secondary uranium mineralisation formed in sandstone or calcrete. Prior to Tianda Resources deciding to apply for...

The central Gawler Craton is blanketed by thin sedimentary cover that ranges in age from Neoproterozoic to Quaternary. Locally, though, such cover can reach a maximum of ~500 m thickness in Permian glacial valleys or rift structures. This guide...

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...

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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...

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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 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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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...

There is no abstract created for this record.

Exploring the earth resources in the Harris Greenstone Belt (HGB) region is complicated by a regolith cover produced by a long and complex history of landscape evolution. The present surface of the HGB indicates little of the complex palaeochannel...

Includes Part 2 - Upper Palaeozoic and Lower Cretaceous micropalaeontology.