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RB 2006/00017 Geological notes on the Coppertop, Montstephen, southern Morialpa and southeastern Plumbago Inliers
Four areas on the south-western margin of the Palaeo-Mesoproterozoic Willyama Inliers were mapped in detail to elucidate the nature of their lithostratigraphy, structure and mineralisation. These basement inliers are composed of...-
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Published: 01 Dec 2006
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RB 2005/00007 Lake Gairdner “section 12 determination” – Mineral Potential
The proposed Lake Gairdner 'section 12 determination' area has the potential to host significant mineral deposits. The area lies close to two major geological boundaries; to the immediate north is the Yerda Shear Zone, and to the west, the Yarlbrinda...-
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Published: 01 May 2005
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RB 2006/00019 Previous exploration and mineral potential of ELA 2002/00154
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...-
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Published: 01 Dec 2006
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RB 2002/00007 The Palaeo-Mesoproterozoic geology of northern Yorke Peninsula, South Australia. Hiltaba Suite - related alteration and mineralisation of the Moonta - Wallaroo Cu-Au district (Resources '96 Convention, Adelaide, geological field excursion
Returns from copper and gold won from the Moonta-Wallaroo district supported the South Australian economy from 1860-1920. During those 60 years some 355,000 t of copper and 2 t of gold were extracted from the twin mining fields of Wallaroo and Moonta:...-
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Published: 01 Nov 1996
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RB 2003/00021 Musgrave Province - Geological summary and exploration history.
The Musgrave Province is largely incorporated within the Anangu Pitjantjatjara Lands and includes cratonic crystalline middle Proterozoic basement rocks of the Musgrave Province proper, as well as mantling younger sedimentary rock successions...-
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Published: 01 Nov 2003
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RB 2003/00013 North-western Murray Basin geological synthesis, South Australia.
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...-
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Published: 01 Aug 2003
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RB 2002/00031 Musgrave Block, central Australia. Regional geology from interpretation of airborne magnetic data.
A regional geological interpretation of newly-acquired magnetic data for the majority of the Musgrave Block (central Australia) has been compiled at 1:250 000 scale. This report outlines the methodology and results of interpretation. Highlights of...-
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Published: 01 Aug 2002
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RB 2007/00010 Investigation of geochemical exploration techniques in the Curnamona Province : CurnaMinEx Project results, 2005-2006.
Thick sediment cover in the Proterozoic Curnamona Province impedes effective mineral exploration in some of the most prospective areas located away from bedrock outcrop. The objectives of the CurnaMinEx project are to test the effectiveness of surface...-
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Published: 01 Dec 2007
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RB 2007/00006 The geology and mineral potential of the PORT AUGUSTA [mapsheet] area, eastern Gawler Craton.
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...-
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Published: 01 Apr 2007
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RB 2014/00005 WINTINNA, South Australia, [geological map] sheet SG53-14. South Australia. Geological Survey. 1:250 000 Series - Explanatory Notes.
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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Published: 01 Mar 2015