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ExpNotes PARACHILNA (v2): Explanatory Notes PARACHILNA (second edition, 1999)
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...-
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Reaphook Hill. Final report at licence surrender, for the period 1/12/1965 to 13/5/1968.
The reported presence of high geochemical zinc values in the Parachilna Formation rocks exposed there prompted Kennecott Explorations to include the Reaphook Hill outlier of Lower Cambrian sediments into its regional investigation of the stratiform...-
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Published: 25 Mar 1967
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Mount Lyall. Progress and final reports to licence expiry/renewal for the period 1/5/1969 to 24/3/1971.
The Third Plain zinc silicate (willemite) deposit, located 14 miles south-east of Blinman, has been newly assessed by North Flinders Mines for its economic potential. Originally discovered by Kennecott Explorations in late 1966, and evaluated by them...-
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Preliminary report on the geology of the Kempes Bore area, eastern Flinders Ranges.
There is no abstract created for this record-
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Reaphook Hill. Progress and final reports to licence expiry/renewal for the period 1/12/1965 to 30/11/1966.
Systematic stream sediment sampling and follow-up surface rock chip sampling has been carried out across the Reaphook Hill outlier of Lower Cambrian sediments to investigate the economic potential of previously reported high geochemical zinc values in...-
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Published: 01 Dec 1966
