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Mount Arden. Progress reports to licence expiry for the period 1/7/1968 to 30/6/1970.
Assays of 21 geochemical samples taken from within Donnelly's iron ore deposits on Mineral Claim 4573 indicate that they have a significant anomalous trace metal content, with up to 0.25% Cu occurring in wallrocks consisting of manganiferous quartzite...-
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Published: 04 May 1970
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Parachilna. Progress reports to licence expiry/renewal for the period 2/4/1970 to 1/4/1971.
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...-
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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...-
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Published: 01 Apr 2007
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Beltana - Aroona region. Progress reports and technical reports to licence expiry/renewal, for the period 16/7/1971 to 15/7/1972.
Continuing prospect exploration work at the Beltana zinc orebody discovery has consisted of detailed geological mapping at 1:4 800 scale, rock chip sampling of outcropping Adelaidean and Cambrian sediments, field investigation of microgravity...-
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Third Plain (east-central Flinders Ranges). Technical report plus final report to licence full surrender, for the period 1/1/1967 to 30/9/1967.
Stream sediment sampling, conducted by Kennecott as follow-up to a 1966 regional surface geochemical reconnaissance programme looking for stratabound Mississippi Valley - type base metal deposits in the central Flinders Ranges, has located a small...-
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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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Willochra. Progress report to licence surrender for the period 1/12/1965 to 31/5/1966.
As part of a regional investigation of the stratiform base metal mineral potential of Cambrian strata in South Australia, Kennecott has undertaken a geochemical reconnaissance of the Parachilna Formation and Wilkawillina Limestone strata present in...-
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Published: 23 May 1966
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Parachilna - Mernmerna area. Progress and final reports to licence expiry/full surrender, for the period 14/6/1966 to 14/11/1969.
Continuing exploration for Ediacara - type, Early Palaeozoic carbonate sediment-hosted lead-zinc deposits in the Bunyeroo Gorge - Parachilna Gorge area of the Flinders Ranges comprised regional and detailed stream sediment, rock chip and soil...-
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Published: 13 May 1969
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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
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ExpNotes PARACHILNA (v2): Explanatory Notes PARACHILNA (second edition, 1999), SH 54-13.
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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