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Tallaringa and Mount Igy (the Tallaringa JV Project). Joint annual reports to licences' joint full surrender, for the period 18/1/2009 to 6/2/2015.
During the 2009-2010 project joint reporting year, the following activities occurred: - the conduct of an Aboriginal heritage work area clearance survey in the northern part of EL 3485 Tallaringa by the Antakarinja Land Management Council Native...-
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Wilkinson Lakes East. Annual reports plus final report to licence full surrender, for the period 3/5/2010 to 6/2/2015.
An area centred ~150 km west of Coober Pedy, that is located mostly north-west of and that also has a small part lying immediately south-east of the Karari Fault, a major crustal structure which has controlled deposition at the southern limit of the...-
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EL 6401 - Billa Kalina area. Annual technical reports from 11/09/2019 to full surrender 27/03/2023.
Exploration Licence 6401 lies in northern South Australia around 600km NNW of Adelaide. The town of William Creek lies around 80km north of the tenement. The tenement sits to the east of the Mt Woods Inlier where a large amount of exploration has...-
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Published: 27 Mar 1923
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Billa Kalina Homestead. Progress reports and final report to licence full surrender, for the period 30/6/1977 to 14/2/1979.
Airborne and ground geophysical surveys were undertaken in the Billa Kalina area, prior to commencing to drill in a search for Olympic Dam type Cu-U-Au mineralised haematitic breccias, in order to delineate and detail several broad magnetic anomalies...-
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Cudyea. Annual reports and final report to licence expiry/full surrender, for the period 2/1/2007 to 1/1/2011.
Mineral exploration conducted in an area centred approximately 125 km west of Tarcoola has addressed targets including possible Challenger type metamorphic gold mineralisation or Olympic Dam type epithermal IOCG mineralisation, and also less deeply...-
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Published: 21 Mar 1911
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ExpNotes GILES: Explanatory Notes GILES
Concealed basement on GILES comprises ?Archaean to Palaeoproterozoic metamorphic rocks belonging to the Nawa Subdomain of the Gawler Craton. These are intruded by Mesoproterozoic Hiltaba Suite granitic bodies and Mesoproterozoic or Neoproterozoic...-
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