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Ferguson [Siding]. Data release made at partial relinquishment of a subsequent licence : annual reports for the period 13/6/1995 to 12/12/2000.
An area located 35 km south-east of Tarcoola was targeted for gold because of interpreted aeromagnetic data, which suggested the presence of discrete Archaean iron formations and mafic rocks within the more widely distributed Kenella Gneiss, a rock...-
Document
Published: 16 Feb 2000
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Data release [made at SA Director of Mines' discretion] : Lake Labyrinth West - Lake Harris West area (the Glenloth JV Project). Annual reports to licence expiry/renewal, for the period 25/5/1998 to 10/7/2008.
Continued exploration for Archaean lode-style gold and Mesoproterozoic Hiltaba Suite granite-related hydrothermal Cu-Au within the retained southern former subarea 'B' of EL 2518 located ~40 km south-east of Tarcoola, where there is also potential...-
Document
Published: 08 Oct 2008
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Kingoonya. Annual reports and final report to licence full surrender, for the period 27/11/2006 to 21/4/2015.
An area surrounding the township of Kingoonya and straddling the Trans Australia Railway line, that comprises six tenement sub-blocks,has been explored for possible economic occurrences of buried Tertiary roll-front style secondary uranium...-
Document
Published: 23 Apr 2015
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Ferguson [Siding]. Data release made in lieu of submitting a third partial surrender report at licence expiry/renewal: annual reports for the period 6/9/2000 to 5/9/2005.
Exploration of an area located about 50 km west of Kingoonya, looking for possible Archaean to Proterozoic mafic intrusive and shear-related economic gold and base metal mineralisation, has lately been hampered financially by the exit of Mount Isa...-
Document
Published: 09 Sep 2005
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Data release [made at SA Director of Mines’ discretion] : Mount Finke. Annual reports including 'no work' letters, for the period 12/8/2015 to 11/8/2018.
An area centred ~45 km south-west of Tarcoola is being explored for possible buried epithermal/hydrothermal copper-gold and magmatic copper-nickel-PGE mineralisation which could have formed within Archaean and Proterozoic basement rocks. During the...-
Document
Published: 09 Oct 2018
