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RB 86/00042 Excursion guide, TARCOOLA 1:250 000 map sheet area.
The geology of 42 outcrops is briefly described. All are Precambrian in age and each site is located on a 1:100 000 geological map.-
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Published: 01 Jun 1986
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RB 2015/00029 What lies beneath the western Gawler Craton? [Eucla-Gawler Seismic Survey line] 13GA-EG1E Seismic and Magnetotelluric Workshop 2015. Extended abstracts [of technical presentations].
This compilation of written and associated oral papers that were presented for the “What lies beneath the western Gawler Craton? 13GA-EG1E Seismic and Magnetotelluric Workshop 2015” is an important step in building our geological understanding of one...-
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Published: 01 Dec 2015
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Data release - as updated [made at SA Director of Mines’ discretion] : Tarcoola. Annual reports for the period 2/6/2008 to 29/7/2018.
During the first year of renewed EL 4167, in October and November 2008, Stellar Resources Ltd ("Stellar") completed a 5 hole, 1286.9 m RC and 2 hole, 157.1 m diamond cored inclined drilling programme at the Coolybring prospect which is located...-
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Published: 11 Sep 2018
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Tarcoola. Final report, Exploration Drilling and Geophysical Component. Project ADI RD02-300 [Accelerated Discovery Initiative Round 2, 2022].
The final report for the Accelerated Discovery Initiative Round 2 is reported in two parts: a geophysical component and an exploration drilling component. Barton Gold Holdings Ltd (Barton), through its wholly own subsidiary Tarcoola 2 Pty Ltd,...-
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Published: 31 Aug 2022
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Whymlet (part of the Mintabyng Project). First partial surrender report, for the period 29/11/2012 to 2/6/2015.
In late November 2012, three adjoining areas in the central Gawler Craton were taken up by Woomera Exploration Limited (WEX), an unlisted public company, for the purpose of minerals exploration. Within the subject licence area which is centred ~30 km...-
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Published: 16 Jun 2015
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Lake Labyrinth. Fourth partial surrender report, for the period 31/10/2001 to 8/2/2011.
Exploration for possible buried epithermal or hydrothermal gold deposits within the large variety of Archaean, Palaeoproterozoic and Mesoproterozoic basement rocks present in an area located 20 km east of Tarcoola has targeted the potential of a...-
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Published: 27 Jun 2011
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Lake Labyrinth (part of the Tarcoola Joint Venture Project). Annual reports to licence expiry/full surrender, for the period 31/10/2001 to 8/2/2012.
Exploration for possible buried epithermal or hydrothermal gold deposits within the large variety of Archaean, Palaeoproterozoic and Mesoproterozoic basement rocks present in an area located from 20-30 km east of Tarcoola has targeted the potential of...-
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Published: 05 Apr 2012
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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
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RB 2019/00008 Gawler Craton Airborne Geophysical Survey Region 9A, Childara – Enhanced geophysical imagery and magnetic source depth models
This report presents the results of a study jointly conducted by the Geological Survey of South Australia and CSIRO Mineral Resources which aimed to enhance the expression of geological structure in geophysical images and to derive depth to magnetic...-
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Published: 01 Apr 2019
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RB 2002/00028 Gawler Craton, 2002. State of play. [Notes to accompany viewing of the ancillary] Drill core display.
This geotechnical workshop of seminars and core displays, which was held over two days on 5-6 December 2002, aimed to highlight recent collaborative research between PIRSA [MER], Geoscience Australia and the South Australian mineral industry that has...-
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Published: 01 Dec 2002
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RB 2004/00001 Palaeochannel studies related to the Harris Greenstone Belt, Gawler Craton, South Australia. Architecture and evolution of the Kingoonya Palaeochannel system.
Exploring the earth resources in the Harris Greenstone Belt (HGB) region is complicated by a regolith cover produced by a long and complex history of landscape evolution. The present surface of the HGB indicates little of the complex palaeochannel...-
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Published: 01 Jun 2004