Sediments in the area mapped belong to the Torrensian Series of the Adelaide System and includes dolomites, phyllites and quartzites, on the east limb of a major anticlinal fold. Some minor folding (interpreted as dragstructures) and faults were seen....

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Sediments in the area mapped in detail belong to the Montacute Dolomite Formation and lower Slate Formation of the Torrensian Series. For the purpose of this report the Lower Slate formation is called the Pinkerton Gully Dolomite formation. Tests...

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Sediments including quartzites dolomites, schists and phyllitic slates of the Torrensian series occur in the above sections. These sediments have been folded into a large anticline on the western limb of which large drags are developed. Pitch change...

Reserves of 12.1 million tonnes of dolomite are indicated, but are conditional upon removal of 2.2 million tonnes of waste dumps and of 5.8 million tonnes of phyllite.

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About 15 miles north-east of Adelaide, the Houghton Inlier composed of older Precambrian schist, gneiss and pegmatite is overlain unconformably by younger Precambrian sedimentary rocks of the Adelaide System. The inlier forms the core of an anticline...

In a search for possible economic base and precious metal mineralisation associated with historic mines located on shear zones in Adelaidean strata, exploration comprising rock chip, soil and stream sediment sampling in the Montacute - Forest Range...