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RB 95/00021 Neoproterozoic depositional sequences and tectonics, eastern Officer Basin, South Australia.
The Officer Basin probably formed when the Gawler Craton collided westerly with the Yilgarn Craton during 1300-1000 Ma; the collision-faulted belt of the Fraser-Musgrave Orogen might form the basement of the Munyarai Trough in the eastern part of the...-
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Published: 01 Jun 1995
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Burial history analysis of the east Officer Basin, South Australia. A preliminary study.
In South Australia, the intracratonic eastern Officer Basin, which may contain up to 10 km of Neoproterozoic to Paleozoic sediments, is bounded by the Precambrian Gawler Craton to the southeast, the Musgrave Block to the north, and passes into...-
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Geochemical measurement of thermal maturity in Neoproterozoic and Cambrian sediments, eastern Officer Basin.
As part of the work of modelling the thermal history of the Ediacaran (Late Neoproterozoic) and Early Cambrian sequences of the eastern Officer Basin that are hosts to oil shows and potential source and reservoir rocks, an essential prerequisite is to...-
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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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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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RB 97/00019 PGSA 003 Petroleum geology of South Australia. Volume 3 - Officer Basin.
This document presents an integration and summary of all new data, and a consolidation of current concepts and ideas on the geological and structural history, sedimentary features and petroleum potential of the Officer Basin in South Australia. Many...-
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Published: 10 Apr 1997
