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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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Cocata and Palkagee Well. Annual reports and final reports to licences' joint expiry/full surrender, for the period 1/12/2005 to 30/11/2010.
Exploration carried out over two adjacent areas located 50 to 70 km south-west and south of Wudinna was progressed under the terms of two separate joint venture agreements made by the licensee in October 2006, firstly with GE Resources (a subsidiary...-
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Published: 27 Jan 1911
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RB 2005/00004 Palynological evidence for late Eocene and late Miocene early Pliocene sediments of Flinders Island, South Australia
Palynological analysis and dating of 45 sediment core samples, obtained from several rotary drillholes that have recently been drilled to explore for buried diamonds and kimberlite indicator minerals on Flinders Island, South Australia, has indicated...-
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Published: 01 May 2005
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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
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RB 2007/00008 CHILDARA, South Australia, [geological map] sheet SH53-14. South Australia. Geological Survey. 1:250 000 Series - Explanatory Notes.
The CHILDARA 1:250 000 map area is located on the western Gawler Craton, an ancient crystalline shield comprising Archaean, Palaeoproterozoic and Mesoproterozoic metasediments, volcanics and granites that has been tectonically stable since 1450 Ma...-
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Published: 01 May 2007
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ExpNotes BARTON: Explanatory Notes BARTON
Shallow Precambrian crystalline basement underlies the greater part of the BARTON 1:250 000 map area. Thicker Neoproterozoic, Cambrian and Carboniferous Permian sediments occur in the northwest, with the southern margin bounded by the Karari Fault...-
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