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RB 91/00041 Geology of the KINGOONYA 1:250 000 map sheet area.
Extensive field geological mapping, augmented by petrological and geochemical studies, reinterpretation of company drilling and water-bore logs and a nine-hole drilling programme has detailed the geology of the KINGOONYA area. The stratigraphy spans...-
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Published: 01 Apr 1991
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Galaxy Tank (part of the Central Gawler Project). Annual reports to licence expiry/full surrender, for the period 22/3/2006 to 10/5/2013.
Tasman Resources' ("Tasman") Central Gawler Project tenement acreage, originally comprising seven exploration licences ELs 3339 to 3345, was initially applied for on the basis of perceived prospectivity for diamonds: however, following Tasman's...-
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Published: 16 Jul 1913
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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 2007/00011 Original full content version of] OOLDEA, South Australia, [geological map] sheet SH52-12. South Australia. Geological Survey. 1:250 000 Series - Explanatory Notes.
The OOLDEA 1:250 000 map area, in the far west of SA, includes portions of the Maralinga Tjarutja Aboriginal Lands, Maralinga Prohibited Area, and Nullarbor Regional Reserve. It is traversed by the Trans-Australian Railway. There is no significant...-
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Published: 01 Jun 2007
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Warrior. Progress reports for the period 4/4/79 to April 1982.
The licence was relinquished following conduct of intensive exploration in the Malbooma area since 1973. Drilling of 514 percussion holes (totalling 21 355 metres) and 29 cored holes (totalling 1 111 metres) defined widespread uranium mineralisation,...-
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Published: 01 Jan 1982
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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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ExpNotes OOLDEA: Explanatory Notes OOLDEA
There is no abstract created for this record-
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