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PACE Discovery Drilling (drilling partnerships with DSD and industry): Year 9 partnership DPY8-30 - Eucla Basin Eocene and Pleistocene low-stand beach ridge marine heavy mineral placer prospects. Drilling project final report.
The Nundroo Range and Bookabie Range are prominent south-west facing, yet effectively previously undrilled, preserved palaeogeomorphic beach ridge /coastal dune features which are located ~200 km west of Ceduna and ~100 km south of the...-
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Pidinga (part of the Eucla-Maralinga Heavy Mineral Sands Project). Annual reports, including those for the commencement of licence joint annual reporting for the Eucla Basin Mineral Sands Tenement Group 1, for the period 27/8/2004 to 28/2/2009.
An area located on the eastern margin of the Eucla Basin, and centred ~60 km north-east of Fowlers Bay, has now been taken under licence by WA-based company Iluka Resources to explore for possible buried economic occurrences of zircon-rich heavy...-
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RB 00855 Maralinga hydrogeological and geotechnical site investigation - Stage 1.
Hydrogeological and geotechnical information is provided for a comparative cost study of competing proposals for the permanent disposal of soil lightly contaminated with nuclear materials. A total of 19 open boreholes and 6 cored boreholes were...-
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Ooldea Range (part of the Eucla Basin Project). Annual reports, including those for the commencement of licence joint annual reporting for the Eucla Basin Mineral Sands Tenement Group 1, for the period 5/3/2002 to 28/2/2009.
The geomorphic feature known as the Ooldea Range, a prominent Eocene dune formed at the limit of the marine transgression on the eastern margin of the Eucla Basin, has now been taken under licence by WA-based company Iluka Resources to explore for...-
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Bookabie area (near Fowlers Bay). Annual, partial surrender and final reports to licence expiry for the period 10/9/2001 to 9/9/2003.
Heavy minerals concentrated within the Ooldea Sand of the Eucla Basin, and possibly reworked and upgraded by later marine incursions into such deposits, which might have led to their redeposition elsewhere as translocated strandlines that are still...-
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