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RB 90/00058 Summary of seismic interpretation in the eastern Officer Basin.
The Proterozoic tectonic evolution of the southern margin of the Eastern Officer Basin is closely related to evaporite mass movements and diapirism. Seismic interpretation suggests that these movements occurred when increased subsidence in the...-
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Published: 01 Oct 1990
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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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Burial history of the eastern Officer Basin, South Australia.
Burial history analysis of the structurally complex eastern Officer Basin region was performed using data from petroleum, trona exploration and stratigraphic wells, seismic upholes, coal drillholes and selected seismic sections, to construct isopachs...-
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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, SH 52-12.
There is no abstract created for this record.-
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