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RB 93/00042 Orroroo bedrock drilling 1993.
Eighty three reverse circulation drill holes totalling 2615.5 metres were drilled on Quorn, Orroroo, Paratoo and Carrieton 1:100 000 sheets to determine bedrock geology and geochemistry below sedimentary cover. The program is a part of the South...-
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Published: 01 Oct 1993
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Eukaby. Progress and final reports to licence surrender for the period 22/6/1972 to 31/5/1973.
As part of North's continuing exploration for possible buried syngenetic, Broken Hill - type stratiform base metal deposits in the Eukaby area, extensive deep directional diamond core drilling (9 of 14 holes totalling 11,603 feet) was carried out in...-
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RB 69/00006 Exploration of the Mount Coffin Diapir, northern Flinders Ranges (logs not published).
Diapiric marbles and dolomitic siltstone breccia of presumed Willouran age intrude younger Umberatana Group rocks which have been folded into an elongate domal structure and, in part, rest unconformably on the diapiric core. Within the diapir several...-
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Published: 01 Jan 1971
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Mount Craig (part of the Hawker Project). Annual and final reports to licence expiry/full surrender for the period 15/11/2005 to 14/11/2010.
Copper Range's principal exploration targets in the Adelaide Fold Belt are secondary, near-surface oxide copper deposits that are structurally controlled and related to hydrothermal events focussed along faults late in the deformational history of the...-
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Published: 06 Apr 1911
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Mount Fitton. Progress and final reports to licence amalgamation/renewal for the period 19/5/1969 to 31/1/1971.
After reviewing the existing Anaconda regional stream sediment geochemical anomalies, North Flinders Mines attempted to replicate the reported high zinc values in the north-east of the licence area, by conducting a higher density reconnaissance stream...-
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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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