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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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Ooldea. First partial surrender report at licence expiry/renewal, for the period 20/9/2009 to 19/9/2014. [No work report].
Four separate licence portions together covering an area of 221 square km or ~42% of the former extent of EL 4565 have been voluntarily relinquished. The perceived prospective Karari Fault Zone and other places which possibly contain buried...-
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Data release - as updated [made at SA Director of Mines’ discretion] : Ooldea. Annual reports to licence expiry/renewal, for the period 1/9/2005 to 31/8/2010.
An area centred ~230 km north-west of Ceduna, in the far north-eastern corner of the Nullarbor Plain, and lying just south of the Ooldea railway siding on the Trans Australian Railway line, is being explored for possible economic buried deposits of...-
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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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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
