An area located ~100 km north-west of Kimba, on the southern margin of the Gawler Ranges, is being explored by Investigator Resources for a variety of styles and types of precious and base metal epithermal mineralisation that may have formed in...

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...

Two contiguous areas located south of the Gawler Ranges, between Buckleboo and Franklin Harbour, were taken up primarily to explore the Early Proterozoic metasedimentary sequence for possible Broken Hill type economic stratiform / hydrothermal base...

All of the south-western tip and hinterland of the Fleurieu Peninsula was taken up to explore for inferred buried IOCG-style copper-gold-uranium mineralisation which, by analogy with properties of the known eastern Gawler Craton occurrences, was...

The Yankalilla coastal and river valley district of the west-central Fleurieu Peninsula was taken up to explore for inferred buried IOCG-style copper-gold-uranium mineralisation which, by analogy with properties of the known eastern Gawler Craton...

The Eukaby mining field area of the eastern Flinders Ranges was explored for Au-Ag-Pb-Zn mineralisation, while geophysical data modelling targetted Olympic Dam style metallogenic systems. Information gained from detailed structural mapping and rock...

Exploration for possible economic concealed Beltana mine type stratabound lead-zinc-(silver) mineralisation, and for other diapiric and associated basic igneous intrusion - related base metal and/or gold occurrences, was carried out over a small area...

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...

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...

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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