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Poondinga. Third partial surrender report, for the period 27/10/2004 to 4/4/2019.
309.6 square km or ~18.77% of the pre-existing area of EL 5564 Poondinga was partially relinquished on 19/2/2019 because in the licensee's view this south-eastern portion of the licence are does not appear to exhibit the geological features required...-
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Published: 12 Apr 1919
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Yellabinna and Poondinga. Respective second partial surrender reports, for the period 27/10/2004 to 13/4/2018.
Two adjoining areas located on the eastern margin of the Eucla Basin, and centred ~60 km north-east of Fowlers Bay, are being explored for possible buried economic occurrences of zircon-rich heavy mineral sands (HMS) that may have been formed along...-
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Published: 31 May 1918
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Sandy Plain. Annual reports to licence expiry/cancellation, for the period 3/12/2007 to 2/12/2010.
An area of the onshore Tertiary Eucla Basin located about 170 km north-west of Ceduna and 50 km north-east of Ooldea Siding on the Trans Australian Railway has been explored for possible economic heavy mineral concentrations formed within shallow...-
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Fowlers Bay North. Annual report plus final report to licence expiry/full surrender, for the period 4/8/2008 to 3/8/2010.
Within an area located approximately 110 km north-west of Ceduna, exploration has primarily been directed at assessing the heavy mineral sands potential of Tertiary Eucla Basin shoreline sediments, with an additional objective of determining the base...-
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Published: 31 May 1911
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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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ExpNotes BARTON: Explanatory Notes BARTON, SH 53-09.
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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