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Coonalpyn (part of the Coonalpyn Joint Venture Project). Annual reports to licence expiry/full surrender for the period 16/10/2006 to 15/10/2008.
To investigate the possible Cu-Ni-PGE mineral sulphide mineralisation potential of a known buried mafic / ultramafic layered igneous intrusive complex situated near Ki Ki in the upper South-East, as well as exploring for base metal mineralisation...-
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Published: 13 Nov 1908
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Ki Ki (part of the Coonalpyn Joint Venture Project). Annual reports and final report to licence expiry/full surrender, for the period 14/10/1999 to 17/1/2009.
To investigate the possible Cu-Ni-PGE mineral sulphide mineralisation potential of a known buried mafic / ultramafic layered igneous intrusive complex situated within the Cambrian Kanmantoo Trough near Ki Ki in the upper South-East, the licensee and...-
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Published: 23 Feb 1909
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PACE Theme 2 (drilling partnerships with PIRSA and industry): Year 1 partnership DPY1-32, Ki Ki intrusion mafic/ultramafic - hosted mineral prospects. Project final report.
To further investigate the Cu-Ni-PGE mineral sulphide potential of a known buried mafic / ultramafic layered igneous intrusive complex situated near Ki Ki in the upper South-East, the licensee of EL 3295 sought PACE Initiative funding to complete two...-
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Brownlow (part of the Padthaway and Black Hills Joint Venture Projects). Annual reports and first partial surrender report to licence expiry/renewal, for the period 26/8/1998 to 25/8/2002.
The area of EL 2544, centred 90 km north-east from Adelaide, was considered to be prospective for porphyry/skarn type and iron oxide - associated copper-gold (IOCG) systems related to high level intrusive igneous plutons. Initial exploration...-
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Published: 27 Jan 1903
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Data release - as updated [made at SA Director of Mines' discretion] : Mannum area. Annual technical reports for period ending 08/09/2018.
EL 5846 covers an area of 462 km2 and is located approximately 70km east of Adelaide. It is located within the Murray Basin, with a basement of poorly outcropping to deeply covered Neoproterozoic and Cambrian Kanmantoo Group sediments and...-
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