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RB 96/00001 Mineral exploration and development in South Australia.
This mineral promotional brochure reviews significant historical developments in South Australia's mineral industry and canvasses the currently recognised mineral potential within the State, for the benefit of local and overseas interested companies...-
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Published: 01 Feb 1996
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Wilkinson. Annual reports plus final report to licence expiry/full surrender, for the period 4/1/1999 to 3/1/2002.
Possible potash and halite resources in evaporite - rich sediment sequences of the Tallaringa Trough, lying at depths that might be suitable for solution mining, were the initial targets of exploration in the Wilkinson Lakes area. Following a...-
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Evaporites in the Officer Basin.
The Officer Basin covers about 300,000 square km and is largely concealed beneath sediments of the Gibson and Great Victoria deserts in western and southern Australia. Approximately two-thirds of the Officer Basin lies in Western Australia....-
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Published: 07 Jan 1998
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Noorina - Area 2. Final report at licence full surrender, for the period 11/10/2012 to 3/10/2014.
An area centred ~200 km north of Cook has been explored for possible buried heavy mineral sands (HM) marine placer accumulations that may have formed along a topographic high that is geographically situated immediately north of the Ooldea Range, and...-
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Published: 19 Aug 1914
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Source rock evaluation of Alinya Formation, Giles 1. Data summary and preliminary interpretation.
Preliminary analysis of 6 core samples from 1237-1266 metres depth in Giles 1 has revealed poor to fair organic richness, low concentrations of extractable organic matter and low hydrocarbon yields. Rock-Eval pyrolysis has confirmed the presence of...-
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Eucla Basin Stratigraphic Drilling Project. Well completion reports.
Four wells, drilled within 36 km of the Hughes and Denman Railway Sidings, explored for a possible Palaeozoic section and/or Upper Proterozoic or older basement, that was expected from Outback's regional gravity survey data to occur at or around...-
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RB 00855 Maralinga hydrogeological and geotechnical site investigation - Stage 1.
Hydrogeological and geotechnical information is provided for a comparative cost study of competing proposals for the permanent disposal of soil lightly contaminated with nuclear materials. A total of 19 open boreholes and 6 cored boreholes were...-
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RB 2014/00005 WINTINNA, South Australia, [geological map] sheet SG53-14. South Australia. Geological Survey. 1:250 000 Series - Explanatory Notes.
The WINTINNA 1:250 000 mapsheet area lies between latitudes 27° to 28° South and longitudes 133°30’ to 135°00’ East. This ~16 400 square km area includes the Marla and Cadney Park settlements, and is crossed by the Stuart Highway and Adelaide to...-
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Published: 01 Mar 2015
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Ooldea. Progress reports and final report to licence expiry/full surrender, for the period 2/9/1986 to 1/9/1991.
Exploration for heavy-mineral sand in Tertiary sediments on the south-western flank of the Ooldea Range comprised geological reconnaissance and RC drilling (81 holes, total 1204 m). Up to 3% titaniferous heavy minerals were reported from drill samples.-
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Yarle Lakes and O'Malley Siding. Progress reports to licences' joint full surrender, for the period 20/6/1980 to 19/12/1981.
Two areas located approximately 45-55 km west of Ooldea were explored for possible buried Olympic Dam - type base metal deposits in poorly known Archaean to Early Proterozoic basement beneath the Eucla and Officer Basin sedimentary sequences. A...-
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ExpNotes WINTINNA: Explanatory Notes WINTINNA
A new generation, first edition WINTINNA 1:250 000 scale geological map and explanatory notes have been published. These documents represent the conclusion of the Geological Survey of South Australia's geological mapping program undertaken in the...-
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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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