This report presents the results of a study jointly conducted by the Geological Survey of South Australia and CSIRO Mineral Resources which aimed to enhance the expression of geological structure in geophysical images and to derive depth to magnetic...

In May 2004 the Minister for the Department of Environment and Heritage purchased Bimbowrie Station pastoral lease. The station was purchased because it encompasses part of the Olary Ranges, which is part of the environmentally important Broken Hill...

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The Murray Basin is an intracratonic basin filled with Cainozoic fluvial to shallow marine sediments. Deposition in the Eocene and early Oligocene was characterised by floodplain and swamp deposits, emplaced with occasional interbeds of shelly clays...

After two years of negotiation with traditional owners and the Anangu Pitjantjatjara Land Council, the Geological Survey Branch of PIRSA's Minerals, Petroleum and Energy Division (MPE) commenced stratigraphic drilling on the 15th May 2002, in the...

The Proterozoic Curnamona Province extends across central eastern South Australia and into western New South Wales. While most of the Province is obscured by younger sedimentary cover regions of exposure are present in the northwest as the Mount...

The PORT AUGUSTA 1:250,000 mapsheet area covers the north-eastern part of the Eyre Peninsula, the northern Spencer Gulf and the south-western Flinders Ranges, and extends from latitude 32°00'S to 33°00'S and longitude 136°30'S to 138°00'S. The main...

The Mount Woods Domain (sometimes termed Mount Woods Inlier) is located ~850 km north of Adelaide along the Stuart Highway. The nearest major population centre is Coober Pedy, which lies ~70 km north-west of the northern domain boundary. Geologically,...

Reconnaissance investigations of outcropping rocks of the western and central Mulgathing Complex reveal a series of pelitic and psammitic sedimentary rocks, interleaved with generally mafic to intermediate composition meta-igneous lithologies. The...

Seven samples of Proterozoic basement rocks, representing syn and post-tectonic leucocratic melts that formed during the Kimban Orogeny within the Donington Suite and within cross-cutting Tournefort Metadolerite mafic dykes on the southernmost Eyre...

High precision geochronological analyses of metamorphic and inherited magmatic zircon grains, which were obtained from stored percussion drillhole samples of a garnet gneiss that occurs within the Commonwealth Hill magnetic anomaly, north-western...

Includes abstracts with the following titles: 1) How magnetotellurics (MT) works, and an overview of new central Australian MT results (Kate Selway) 2) Latest MT traverse results: western Gawler Craton (Stephan Thiel) 3) A constrained 3D...

ELA 2002/00154 is made up of three geographically separate sub-areas aligned in a north-easterly direction along the Bulgunnia Shear Zone. Neither the northern nor the central sub-areas have any basement rock outcrop, with the depth of younger cover...

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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This bulletin contains geochronological data and interpretations from the Gawler Craton of South Australia that have been completed by Mark Fanning of The Australian National University, by Geological Survey of South Australia personnel, and by...

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...

There is no abstract created for this record.

There is no abstract created for this record.

There is no abstract created for this record.