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RB 79/00088 Wilkinson 1. Well completion report.
Wilkinson 1 stratigraphic well was drilled by the SA Department of Mines and Energy in mid-1978, about 250 km south-west of Coober Pedy, in the Tallaringa Trough. Here a thick section of Cambrian claystones, limestones and evaporites, at least 594 m...-
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Published: 01 Oct 1979
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RB 99/00031 Assessment of zinc-lead prospectivity on the Murnaroo Platform and in the Manya Trough, eastern Officer Basin, South Australia.
The Neoproterozoic to Palaeozoic Officer Basin is located on and adjacent to the northwestern margin of the Gawler Craton. Deposition of the basin began in Adelaidean time, before and during the breakup of the supercontinent Rodinia. The...-
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Published: 01 Dec 1999
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Sedimentology of the Ouldburra Formation (Early Cambrian), northeastern Officer Basin.
The Ouldburra Formation (Early Cambrian) is a newly defined sequence of carbonates, mixed carbonate/siliciclastics and evaporites in the northeastern Officer Basin, northern South Australia. Deposition took place during the late stages of...-
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ELs 730 - 739, Great Victoria Desert (CRAE Wyola Project). Progress and final reports for the period 6/10/1980 to 14/9/1981.
Compilation and re-interpretation of open file data from the Eucla Basin - southern Officer Basin region preceded exploratory and stratigraphic percussion drilling undertaken in an area north of the Trans Australian Railway (6 holes, total 1032 m)....-
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Published: 09 Jul 1981
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Helicopter reconnaissance of the Emu area, 3/6/82 - 11/6/82. Appendix 1 to quarterly report for period ending 8/2/83.
Bedrock outcrops were mapped at 61 sites spread over 7550 square km of the Great Victoria Desert, including many that had previously been geologically mis-interpreted, or had never before been visited. The sedimentary depositional environment of the...-
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RB 2004/00012 Deposition and chemical composition of Early Cambrian salt in the eastern Officer Basin, South Australia
In South Australia, Cambrian massive salt deposits of the eastern Officer Basin occur in troughs lying along the western and north-western margins of the Gawler Craton, and are considered to have been deposited in marginal to open marine environments....-
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Published: 01 Jul 2004
