A very small area centred ~60 km south-east of Olary has been explored for possible economic buried Late Proterozoic sediment-hosted or volcanic hosted massive sulphide (VHMS) Cu (-Co) mineralisation. Previous exploration conducted by Longreach Metals...

[ Note - here is Part 1 of the abstract relating to 2 separately indexed parts ]. As an adjunct to its widespread search for possible diamondiferous kimberlite diatremes on its Abminga Project acreage situated nearby to the north-west, Caldera...

Newmont Mining used a ground magnetic survey, an IP survey and a soil geochemical survey to select sites at the Mutooroo Ridge copper prospect for its subsequent drilling during May and October 1977 of 2 inclined, percussion precollared diamond cored...

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...

The extremely thick succession provides one of the most complete sedimentary records for the Late Proterozoic. The term geosyncline is used in a non-genetic sense for the basin in which deposition occurred during the Adelaidean and Cambrian. Only the...

The revised digital geology map of the Cultana 1:100 000 map sheet and accompanying geological descriptions in this report are the first components of the 2nd edition PORT AUGUSTA 1:250 000 map sheet to be completed. The subject map sheet occupies the...

The MARREE mapsheet area includes the south-western portion of the Strzelecki Desert plus parts of the Tirari Desert, north-western Flinders Ranges and north-eastern Willouran Ranges, between latitudes 29 to 30 degrees S and longitudes 138 to 139...

The CALLABONNA map area includes the southern end of the Strzelecki Desert and the north- eastern Flinders Ranges, between latitudes 29° to 30° S and longitudes 139° 30' to 141° E. Cameron Corner adjoins New South Wales and Queensland in the...

Exploration for Proterozoic sedimentary-hosted mineral and energy resources can greatly benefit from geochronological methods that date the depositional age of sedimentary rocks that predate the Early Cambrian evolution of biomineralizing organisms....

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A new generation, second edition MARREE 1:250 000 scale geological map and its explanatory notes have been published. These documents represent the conclusion of the Geological Survey of South Australia's latest geological mapping program (1993 to...