The Duntroon Basin is located in the centre of the Southern Rift System between the Bight and the Otway Basins, west and SW of Kangaroo Island. It is limited to the north by the Proterozoic Gawler Craton. The formation of the basin is related to the...

Sedimentation in the Great Australian Bight (GAB) has occurred in a variety of settings from the initial intra-cratonic rift to the modern carbonate shelf. An extensive palaeodrainage system, remnants of which are still preserved, supplied clastic...

This EPP 26 surrender report has been furnished to the SA offshore Designated Authority as a result of the application made on 21/8/96 by BHP Petroleum for permission for the joint venture to surrender the permit, before committing to unwanted...

EPPs 10 and 11 currently comprise 239 graticular blocks (approximately 17 000 sq km) in the Great Australian Bight Basin. No wells have yet been drilled in these permits which lie entirely in water depths greater than 200 m and ranging down to 1 500...

Three structural closures have been defined by the R 10 survey. These are Galah in Permit SA-11 and Kookaburra West and Kookaburra East in Permit SA-10. Economic evaluation of the structures is currently being undertaken, but it is considered in the...

This report provides a brief summary of the geology and petroleum potential of the onshore, South Australian portion of the Eucla Basin at the time of termination of PEL 4, with the aim of providing a starting point for more thorough studies.

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...

The Cenozoic Eucla Basin is located on the southern margin of the Australian continent, with a present-day basin onshore edge which extends for over 2,000 km from Western Australia into South Australia. The basin’s sediment fill comprises a thin...

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