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RB 2018/00001 Regolith hand specimen atlas for South Australia
This regolith material hand specimen atlas displays 246 images of 212 regolith samples which have been collected over the last 30 years by the authors, present and past Geological Survey of South Australia (GSSA) staff and members of the Cooperative...-
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Published: 01 May 2018
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Data release - as updated [made at SA Director of Mines' discretion] : Glenloth area (the Tarcoola JV Project). Annual reports for the period 11/7/2008 to 2/11/2018.
A biogeochemical sampling survey consisting of 20 lines (407 samples) was undertaken by the JV partners during August 2009, targeting buried gold mineralisation. Black Oak and Pearl Bluebush were the dominant deep-rooted plant species sampled and, to...-
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RB 2007/00017 The geology of the Mulgathing Complex: from eastern Tallaringa to Glenloth Goldfield.
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...-
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Published: 01 Sep 2007
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RB 2003/00010 Regolith characterisation and geochemistry as an aid to mineral exploration in the Harris Greenstone Belt, central Gawler Craton, South Australia.
Komatiitic greenstones were first recognised in South Australia from drillcore at Lake Harris on the Gawler Craton by Mines and Energy SA personnel in 1991. Subsequent petrography and detailed aeromagnetic data interpretation led to targeted drilling...-
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Published: 01 May 2004
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RB 2007/00008 CHILDARA, South Australia, [geological map] sheet SH53-14. South Australia. Geological Survey. 1:250 000 Series - Explanatory Notes.
The CHILDARA 1:250 000 map area is located on the western Gawler Craton, an ancient crystalline shield comprising Archaean, Palaeoproterozoic and Mesoproterozoic metasediments, volcanics and granites that has been tectonically stable since 1450 Ma...-
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Published: 01 May 2007
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RB 2007/00015 Geochronology of the Gawler Craton, South Australia.
Geochronology enables us to determine the age of rocks and minerals. The variety of isotopic geochronological techniques give complementary information on, for example, the timing of igneous or metamorphic crystallisation, as is often the case for the...-
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Published: 01 Sep 2007
