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Mount Roebuck. Progress and final reports to licence surrender for the period 28/3/90 to 29/10/91.
TARGET: Diamonds, gold and copper in the Mount Roebuck area. EXPLORATION: Drainage, loam and rock chip sampling, ground magnetic, radiometric and IP surveys, and diamond drilling (4 holes totalling 739 m). RESULTS: A single, 0.5 mm x 0.4 mm diameter...-
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Published: 15 Nov 1991
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Mount Michael. Annual report and final report to licence expiry/full surrender, for the period 7/9/1997 to 6/9/1999.
Interpretation of magnetic and gravity data, together with calcrete and MMI sampling, were carried out adjacent to a southerly extension of the Ediacara Fault, 25 km north-west of Parachilna. Low order Pb-Zn-Ag anomalism was located, coincident with...-
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Published: 10 Nov 1999
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Angepena. Progress and final reports to licence expiry/full surrender for the period 18/12/1969 to 17/12/1970.
In a continuation of the evaluation of the Mucatoona copper prospect, assaying of RAB drill cuttings samples returned no metal values of note. Mineragraphic studies of the primary copper mineralisation occurring in the Adelaidean black shale facies...-
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Angepena. Progress and technical reports to licence expiry/renewal for the period 18/12/1967 to 17/12/1969.
Geological and geochemical investigations undertaken in the vicinity of the historic Mucatoona copper occurrence indicate that the Angepena ?diapiric breccia zones have no potential for hosting economic mineralisation. There is only a marginal...-
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Angaston - Sedan Hill area. Progress reports and final report to licence expiry/full surrender, for the period 18/11/1975 to 17/11/1976.
Regional stream sediment and rock chip geochemical sampling of an area extending from 15 km north-east to south-east of Angaston was undertaken to search primarily for stratabound Mississippi Valley style Pb-Zn mineralisation in lower Cambrian Hawker...-
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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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