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Spencer Gulf. Progress reports to licence expiry/full surrender, for the period 12/2/1981 to 11/2/83.
A 900 line km detailed aeromagnetic survey was carried out over the northern extremity of Spencer Gulf, in a search for possible Olympic Dam style mineralisation associated with a significant and complex magnetic high anomaly that is located almost...-
Document
Published: 15 Jun 1982
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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...-
Document
Published: 01 Apr 2007
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RB 2016/00014 Geology of the Six Mile Hill 1:75 000 Special Edition Map Sheet.
The Six Mile Hill 1:75 000 Map Sheet was produced as part of a mapping program integrated into the Mineral Systems Drilling Program (MSDP) along the southern margin of the Gawler Ranges. The objective of the mapping program was to provide a regional...-
Document
Published: 01 Dec 2016
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Surface Geology of Six Mile Hill – Mineral Systems Drilling Program Special Map Series, 1:75 000 scale.
There is no abstract created for this record-
Map
Published: 01 Dec 1916
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RB 2015/00021 Stratigraphy of the lower Gawler Range Volcanics in the Roopena area, north-eastern Eyre Peninsula.
The Mesoproterozoic (~1590–1586 Ma) Gawler Range Volcanics (GRV) comprise a sequence of A-type dominantly felsic volcanic rocks which were extruded in the central part of the Gawler Craton as part of a volcano-plutonic Silicic Large Igneous Province...-
Document
Published: 01 Dec 2015
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Geology of the Roopena and Uno 1:100 000 sheet areas, eastern Gawler Craton.
This report describes the results of a MESA consultant's second generation regional geological mapping and drillhole data interpretation work for the Roopena and Uno 1:100 000 sheets on PORT AUGUSTA, performed during 1993 and 1994 as part of the SAEI...-
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