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Chundie Swamps. Progress reports and final report to licence expiry/full surrender, for the period 20/8/1986 to 19/8/1987.
The heavy mineral potential of Tertiary sediments in the Chundie Swamps was investigated with 2 drill traverses (43 RC open vertical holes totalling 863 m) and reconnaissance soil mineralogical sampling. Heavy mineral contents were very low.-
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RB 73/00085 Preliminary notes on the geology of the eastern margin of the Eucla Basin, FOWLER 1:250 000 sheet area.
This report deals with the stratigraphy and economic geology of an area on the eastern margin of the Eucla Basin and the western margin of the Gawler Block. The area is centred upon the FOWLER 1:250 000 map area. The stratigraphic section of the...-
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Published: 01 Jan 1973
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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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Ooldea. Progress and final reports to licence expiry/full surrender, for the period 16/11/1972 to 15/11/1973.
In a search for possible economic roll-front sedimentary uranium deposits thought to be hosted by Middle Eocene Pidinga Formation fluvial and lacustrine terrestrial sediments deposited in the eastern Eucla Basin, 13 scout RAB/RC open holes were...-
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RB 2022/00011 Eucla Basin and peripheral paleovalleys.
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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Published: 01 Nov 2022
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ExpNotes OOLDEA: Explanatory Notes OOLDEA
There is no abstract created for this record-
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ExpNotes BARTON: Explanatory Notes BARTON
Shallow Precambrian crystalline basement underlies the greater part of the BARTON 1:250 000 map area. Thicker Neoproterozoic, Cambrian and Carboniferous Permian sediments occur in the northwest, with the southern margin bounded by the Karari Fault...-
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