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Reconnaissance geochemical sampling of the eastern PARACHILNA mapsheet area for sediment-hosted base metal deposits has succeeded in locating several well-defined areas of interest, although approximately two-thirds of the SML area appears to be...

Report presents the results of eight weeks (August-September 1977) spent in the licence area under application, measuring and describing nine stratigraphic sections, with the aim of examining possible sedimentary controls on the known widespread...

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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...

3 sets of fault trends are distinguished, representing the Arrowie fault zone and components of the Mount John, Mount Roebuck and Narina fault zones. Small mineral deposits consist of phosphate, barite and copper.

The Parachilna 1:250 000 map area is about 250 road miles north of Adelaide, South Australia, and includes the eastern shore of Lake Torrens, the central Flinders Ranges and part of the Lake Frome Plains. The ranges are composed of folded Adelaidean...

New stratigraphic units which include the Ediacara fauna are defined and described in section measured in Bunyeroo Gorge.

Seven holes drilled to a maximum depth of 195 ft. (59 m) tested part of the Mt. John Paralana Fault zone for mercury. No anomalous concentrations of mercury were detected. Three holes tested the Parachilna Formation west of the Moro Mine. Anomalous...

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The LINDSAY 1 :250 000 sheet area occupies parts of the southern Musgrave Block and the northern Officer Basin, in the North West Province of South Australia. It is entirely contained by the Great Victoria Desert. The oldest rocks are gneisses of...

This is a new name applied to a Late Precambrian sequence of red and white sandstone which is found in the North West Province of South Australia. It is equated to the Pound Quartzite of the Adelaide Geosyncline on both lithological and fossil evidence.

Investigations on general groundwater potential of the Hawker area were carried out with special attention being paid to the Hookina Creek, Worro Downs - Wonoka Creek, Glen Oak - Willow Creek, Mount Craig areas. An improved supply of water for the...

Copper Range's interest in the Adelaide Fold Belt is predominantly focussed on exploration for copper, as near-surface oxide deposits and sediment-hosted stratiform sulphide mineralisation. However, EL 3646 covering an area adjacent to the south-west...

Copper Range is exploring a number of the Springfield Project mineral tenements for base and precious metals under the terms of a joint venture agreement that it made with licensee Flinders Diamonds on 19/3/2007, whereby the latter retains all rights...

An area located approximately 40 km north-west of Hawker in the southern Flinders Ranges has been explored by Copper Range as part of a regional programme being conducted in the central Adelaide Geosyncline, which is targeting large alteration zones...

Copper Range's interest in the Adelaide Fold Belt is predominantly focussed on exploration for copper, where it may occur as near-surface oxide deposits and as sediment-hosted stratiform sulphide mineralisation. However, EL 3646 was originally applied...

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...

Surveys recently conducted in England, Ireland and Australia have shown that there are major spatial variations in the 'light' [molecular weight] hydrocarbon gas content of rocks which are closely related to the presence of underlying mineralisation....