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Weekeroo. Progress reports to licence expiry/full surrender, for the period 1/10/1970 to 30/9/1971.
A detailed examination of mineralised rock sequences within the metamorphosed Precambrian basement and Adelaidean cover rocks of the Weekeroo area, and recording of their relationship to successive deformational events and resulting rock structures,...-
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Published: 01 Sep 1971
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Wiawera. Annual reports and final report to licence expiry/full surrender, for the period 13/12/1996 to 12/12/2001.
Exploration for possible sheeted vein type gold, Telfer - style gold, and BIF hosted gold and base metal sulphide deposits that may have formed in Adelaidean metasediments occupying the area between Anabama and Radium Hill, 10-30 km south-east of...-
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Anabama Hill. Progress reports and final report to licence expiry/full surrender, for the period 12/11/1990 to 11/11/1991.
TARGET: Possible Starra (Nth Qld) - type gold deposits associated with regional scale structures and associated intrusive rocks in the Anabama Hill region. EXPLORATION: Photogeology studies, reconnaissance BLEG stream sediment (44) and rock chip (16)...-
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Macdonald Hill. Progress reports and final report to licence expiry/full surrender, for the period 13/11/1979 to 12/11/1980.
Base metal exploration carried out over an area extending from 8 to 20 km north-northeast of Olary has consisted of a in-depth technical review of past exploration results, plus limited 1:10,000 scale geological mapping, bulk sampling of...-
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RB 2007/00006 The geology and mineral potential of the PORT AUGUSTA [mapsheet] area, eastern Gawler Craton.
The PORT AUGUSTA 1:250,000 mapsheet area covers the north-eastern part of the Eyre Peninsula, the northern Spencer Gulf and the south-western Flinders Ranges, and extends from latitude 32°00'S to 33°00'S and longitude 136°30'S to 138°00'S. The main...-
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Published: 01 Apr 2007
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Manna Hill. Progress reports to licence expiry/renewal, for the period 8/10/1970 to 7/10/1971.
Exploration for possible economic base metal sulphides hosted within a 10 square mile block of Carpentarian basement schists and gneiss, or within adjoining younger Adelaidean metasedimentary cover rocks, in an area located just north and west of...-
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