Includes Part 2 - Upper Palaeozoic and Lower Cretaceous micropalaeontology.

The South Australian Department of Mines drilled seven stratigraphic wells between 1969 and 1971 in the Arckaringa Basin. This study presents the stratigraphic information obtained and attempts to collate all available information in a syntheses of...

An area centred ~85 km south-southeast of Coober Pedy, at the southern margin of the Lake Phillipson Trough, a long active tectonic feature now occupied by deep sedimentary fill, was taken up by a wholly-owned subsidiary to Monax Mining Ltd primarily...

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...

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...

Late Palaeozoic sedimentary rocks of the Arckaringa Basin in northern South Australia include diamictite and sandstone units of the Boorthanna Formation that were deposited as lodgement till under fluvioglacial conditions. The clast size and matrix...

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...

There is no abstract created for this record.

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...