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Leigh Creek Coalfield, Lobe B coal deposit: SADME/ETSA 1978 coal appraisal drilling program. Data package of coal seam representative sampling results [to be augmented as relevant retained records become rediscovered and made available].
There is no abstract created for this record-
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Published: 01 Jan 1978
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Orroroo (part of the Walloway Project). Annual reports to licence full surrender, for the period 18/3/2010 to 14/5/2014.
A large area consisting of two separate sub-blocks that were centred ~90 km east and 110 km south-east of Port Augusta has been explored for possible economic Tertiary lignitic coal deposits that may have formed in the southern part of a now uplifted,...-
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Published: 13 Aug 1914
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Walloway (part of the Walloway Project). Annual reports to licence expiry/full surrender, for the period 12/5/2008 to 11/5/2014.
An area centred ~90 km south-east of Port Augusta has been explored for possible economic Tertiary lignitic coal deposits that may have formed in the southern part of a now uplifted, ~50 km long x ~15 km wide intramontane sedimentary basin, the...-
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Published: 11 Jul 1914
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Yarley. Annual reports to licence expiry/full surrender, for the period 19/8/2009 to 18/8/2012.
A small area located on the southern Lake Torrens Plains immediately west of the ABC Range was taken up to allow evaluation of its potential for having buried economic sedimentary coal and/or uranium mineralisation occurrences. There are no...-
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Published: 02 Sep 1912
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Wilmington. Progress and final reports to licence expiry/full surrender for the period 23/8/1982 to 22/8/1983.
Exploration was carried out 50 km east of Port Augusta to try to locate possible concealed Triassic coal-bearing basins similar to the nearby Boolcunda and Springfield basins, and to assess the potential for economic Cainozoic lignite occurrences....-
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ExpNotes PARACHILNA (v2): Explanatory Notes PARACHILNA (second edition, 1999)
The PARACHILNA map area (31 to 32°S, 138 to 139.5°E) occupies the central Flinders Ranges which are made up of folded, mostly marine sedimentary Neoproterozoic and Cambrian rocks of the Adelaide Geosyncline, and adjoining plains underlain by Cainozoic...-
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