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RB 77/00107 Evolution of the Middle Proterozoic Chandabooka Caldera, Gawler Range acid
Volcanism associated with the Middle Proterozoic Gawler Range acid volcano-plutonic province was initiated in the Kokatha area by the construction on Archaean basement of a large stratovolcano composed mainly of tholeiitic basalt and potassic basaltic...-
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Published: 20 Sep 1977
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Data release [made at SA Director of Mines' discretion] : Bulgunnia (part of the Gawler JV Project). Annual reports for the period 19/11/1997 to 1/1/2013.
Within an area of the Wilgena and Christie Domains centred 40 km north of Tarcoola, exploration is continuing for Archaean to Proterozoic basement-hosted epithermal, hydrothermal and metamorphic type gold and base metal occurrences. Here an 841 square...-
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Gilles Downs. Annual reports to licence full surrender, for the period 15/2/2012 to 3/5/2016.
An area centred ~90 km south-west of Port Augusta has been explored for possible buried economic epithermal silver mineralisation and porphyry style Cu-Au mineralisation similar to that found recently by Investigator Resources at the Paris deposit...-
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Published: 01 Oct 1916
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Data release - as updated [made at SA Director of Mines' discretion] : Wartaka, Iron Knob, Reid Lookout and Old Wartaka (the Parkinson Dam Project). Annual reports and joint annual reports for the period 17/2/2005 to 26/4/2019.
Four small, adjacent licences located on the south-eastern, shallow subcrop margin of the Gawler Ranges, which together make up an area centred about 25 km north-east of Lake Gilles and 60 km west of Port Augusta, are being explored for possible...-
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Published: 30 Apr 1918
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Data release - as updated [made at SA Director of Mines' discretion] : Old Wartaka. Annual reports for the period 8/5/2013 to 7/5/2019.
A small area located on the eastern side of the Roopena Fault Zone, proximal to the south-eastern margin of the Gawler Ranges, is being explored for possible buried epigenetic gold and silver mineralisation, or IOCG type base metal sulphide...-
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Published: 13 May 1919
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Uno Range (part of the East Eyre Peninsula Project). First partial surrender report, for the period 1/8/2011 to 31/7/2018.
A licence consisting of two separate sub-blocks located ~30 km west-northwest of Iron Knob is being explored for possible economic buried Paris type epithermal/hydrothermal gold and silver mineralisation, as well as for Menninnie Dam type...-
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Published: 05 Oct 1918
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Data release (in part made in lieu of submitting a second partial surrender report) : Uno Range (part of the East Eyre Peninsula Project). Annual reports for the period 1/8/2011 to 31/7/2020.
A licence consisting of two separate sub-blocks located ~30 km west-northwest of Iron Knob is being explored for possible economic buried Paris type epithermal/hydrothermal gold and silver mineralisation, as well as for Menninnie Dam type...-
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Published: 18 Dec 1920
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Data release - as updated : Western Lake Gairdner. Annual reports and final report to licence expiry/full surrender, for the period 22/2/2011 to 21/2/2018.
An area centred ~100 km south-east of Tarcoola is being explored for possible economic buried Carrapateena or Prominent Hill style IOCG and polymetallic skarn style mineralisation which may be associated with zones of elevated relief seen in existing...-
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Published: 29 May 1918
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Data release - as updated : Lake Harris. Annual reports to licence expiry/full surrender, for the period 15/2/2012 to 14/2/2019.
An area centred ~90 km south-east of Tarcoola and adjacent to the western shore of Lake Gairdner is being explored for possible economic buried Carrapateena or Prominent Hill style IOCG and polymetallic skarn style mineralisation which may be...-
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Published: 20 Mar 1919
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Lake Harris. First partial surrender report at licence expiry/renewal, for the period 15/2/2012 to 14/2/2017.
An area located immediately south-east of Lake Harris and north-west of Lake Gairdner is being explored for possible buried economic basement-hosted Carrapateena/Prominent Hill style IOCG/polymetallic skarn style mineral deposits associated with zones...-
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Data release - as updated [made at SA Director of Mines' discretion] : Morgans (part of the East Eyre Peninsula Project). Annual reports for the period 17/1/2012 to 16/1/2019.
An area of mainly covered bedrock consisting of two separate sub-blocks bordering the south-eastern Gawler Ranges, which is considered prospective for finding buried hypogene IOCG mineralisation and possible stratiform and metamorphic base metals in a...-
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Published: 21 Mar 1918
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Data release - as updated : Mount Nott. Annual reports to licence expiry/full surrender, for the period 17/1/2012 to 16/1/2019.
An area located ~100 km north-west of Kimba, on the southern margin of the Gawler Ranges, is being explored by Investigator Resources for a variety of styles and types of precious and base metal epithermal mineralisation that may have formed in...-
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Published: 26 Mar 1919
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PACE Discovery Drilling (drilling partnerships with DSD and industry): Year 8 partnership DPY8-12 - Corunna Station, north-eastern Eyre Peninsula, structurally controlled Mesoproterozoic epithermal Ag-Au and base metal prospects. Drilling final report.
Musgrave Minerals Ltd (MGV) is the holder of the subject EL 5497 Corunna North, located in the southern Gawler Ranges approximately 65 km west of Port Augusta and 10 km north of Iron Knob, where it is exploring for economic base and precious metal...-
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Data release [made at SA Director of Mines' discretion] : Mount Ive Project. First annual report, for the period 1/1/2016 to 31/12/2016.
The “Mt Ive Project” forms the western part of the “Gawler Ranges Project”. The “Gawler Range Project” comprises 11 tenements covering a total area of 4,749 km2 in northern Eyre Peninsula. All 11 tenements are licenced to and operated by Menninnie...-
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Data release - as updated [made at SA Director of Mines' discretion] : Kolendo, Taringa, Nonning, Wipipippee and Menninnie Dam (the Menninnie Project). Joint annual reports for the period 1/1/2013 to 31/12/2016.
The Menninnie JV Project area consists of five contiguous exploration licences, and is considered prospective for Pb-Zn-Ag-Cu-Au-Mo-U deposits associated with past epithermal, porphyry, IOCG and skarn - forming geological environments. It lies in a...-
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Pernatty. Annual reports to licence expiry/full surrender, for the period 20/3/2018 to 19/3/23.
The Pernatty Project is located approximately 20 km SSE of the IOCG deposit at Carrapateena, within Exploration Licence 6137. The area was initially targeted by Tasman Resources Ltd due to available geophysical data, the possibility of reasonable...-
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Published: 25 Mar 1923
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Kokatha prospect final report.
27 rotary drill holes (total 213m.) tested for copper-nickel mineralisation associated with a gabbro margin. It was concluded that copper-nickel values of several hundred parts per million is restricted to a small area near the gabbro/hornfels...-
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Published: 01 Jan 1969
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Lake Gilles. Final report at licence full surrender, for the period 1/12/2005 to 7/10/2010.
EL3466, located approximately 10 km west-southwest of Iron Knob, was taken up primarily to search the Proterozoic basement for possible buried Olympic Dam style Cu-Au-U mineralisation. Secondary exploration targets included orogenic lode gold...-
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Published: 02 Jun 1911
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Wartaka [Homestead] (part of the Parkinson Dam Project). Annual reports [to the commencement of project licences' combined reporting] and final report to licence surrender, for the period 20/6/2003 to 30/6/2012.
An area located approximately 50 km west of Port Augusta has been explored for economic epithermal gold and silver mineralisation following the discovery of such mineralisation a short distance to the north on the licensee's adjoining EL 3307 / 4475....-
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Mount John, Blue Dam and Blue Dam West (the Acraman Project). Joint first annual report, plus final report to licences' joint full surrender, for the period 10/9/2012 to 9/9/2014.
Licence areas consisting of several small sub-blocks that were located north and north-west of Lake Acraman have been explored for possible epithermal silver-gold and porphyry copper mineralisation that may have formed within altered lower Gawler...-
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