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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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Eastern Officer Basin geology and hydrocarbon potential.
Following the allocation in 1992 of Aust $2 million to MESA for petroleum exploration as part of the SA Exploration Initiative, the Department undertook to conduct reconnaisance seismic surveys over selected, poorly known sedimentary basins. As part...-
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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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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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ExpNotes OOLDEA: Explanatory Notes OOLDEA
There is no abstract created for this record-
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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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