An area located approximately 50 km east of William Creek and abutting the western shoreline of Lake Eyre North was taken up to explore for possible concealed IOCG style base metal and uranium deposits, that could have formed in buried Archaean to...

Two contiguous exploration licences, ELs 6522 and 6523, were secured in the Yudnapinna district to apply new concepts and techniques aimed at revitalising the rate of copper-gold mineral deposit discovery in South Australia. The licences’ area lay...

Two contiguous exploration licences, ELs 6522 and 6523, were secured in the Yudnapinna district to apply new concepts and techniques aimed at revitalising the rate of copper-gold mineral deposit discovery in South Australia. The licences’ area lay...

Nine compact seismic motion recorders and nine co-located ground probe thermocouples have been deployed at various sites near the Carrapateena mine, to test the efficacy of making continuous remote data collection and the reliability of their...

The subject map presents a weights of evidence mineral prospectivity analysis of the Olympic Cu–Au Province in the eastern Gawler Craton. This metallogenic province is host to iron oxide – copper gold (IOCG) deposits including Olympic Dam and...

Hallett Cove is one of South Australia’s foremost natural science treasures. Exposed examples for prime geological concepts of superposition of strata, depositional unconformities (representing time breaks), and folding and faulting of sedimentary...

Following the farm-in of Anglo American Exploration to this tenement in March 2003, new activity has focussed on the rapid definition of drilling targets in a search for possible Archaean basement volcanic or sediment-hosted base metal massive...

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A strong total count radiometric anomaly (to 10 x background) was encountered on the western shoreline of Lake Torrens, about 20 miles south-east of Andamooka, during the course of reconnaissance aerial radiometric surveying. Detailed tests to...

Geochemical and isotopic data from mantle-derived mafic rocks provide important constraints on our understanding of the composition and evolution of the lithosphere through time. Since the lithosphere is sensitive to tectonic processes such as...

During the period 1745–1700 Ma, felsic and mafic rocks were intruded throughout the Gawler Craton, broadly coeval with the 1740–1690 Ma Kimban Orogeny. These rocks were previously considered part of the Lincoln Complex, a stratigraphic term defined by...

Large potential field anomalies can be observed in the Marla region of northern South Australia, and have been used to define the northern limit of the Gawler Craton. The subject project’s aim was to model the plausible source(s) for each of those...

This report book contains SHRIMP zircon U-Pb geochronological data obtained between July 2007 and June 2009, for 10 metasedimentary and meta-igneous rocks from the Mulgathing Complex of the north-estern Gawler Craton. The geochronological study was...

This compilation of written and associated oral papers that were presented for the “What lies beneath the western Gawler Craton? 13GA-EG1E Seismic and Magnetotelluric Workshop 2015” is an important step in building our geological understanding of one...

Large potential field anomalies can be observed in the Marla region of northern South Australia, and have been used to define the northern limit of the Gawler Craton. The subject project’s aim was to model the plausible source(s) for each of those...

Upper crustal strata forming the northern to central Flinders Ranges area comprise uplifted and eroded remnants of openly folded sedimentary rocks that were deposited in an intra-continental arm of the Neoproterozoic to Early Cambrian Adelaide...

The northern to central Flinders Ranges area comprise uplifted and eroded remnants of openly folded sedimentary rocks that were deposited in an intra-continental arm of the Neoproterozoic to Early Cambrian Adelaide Geosyncline. Deposition was...

South Australia’s Olympic Cu-Au Province hosts some of the world’s great iron oxide copper gold (IOCG) deposits, such as Olympic Dam, Prominent Hill and Carrapateena. The same causative thermal event resulted in variants of this deposit class being...

Upper crustal strata forming the northern to central Flinders Ranges area comprise uplifted and eroded remnants of openly folded sedimentary rocks that were deposited in an intra-continental arm of the Neoproterozoic to Early Cambrian Adelaide...

The northern to central Flinders Ranges area comprise uplifted and eroded remnants of openly folded sedimentary rocks that were deposited in an intra-continental arm of the Neoproterozoic to Early Cambrian Adelaide Geosyncline. Deposition was...