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PEL 47. Progress and technical reports for the period June 1990 to March 1993.
Anzoil NL carried out geological and geophysical studies on previous exploration data, but was unsuccessful in attracting farmin partners either locally or overseas. The licence area was reduced to ease the work commitment, by partial relinquishment...-
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Published: 31 Mar 1993
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RB 2002/00024 Sequence analysis and petroleum potential in the Arrowie Basin, South Australia.
Cambrian sediments in the Arrowie Basin were deposited on a rifted continental margin. Four distinct depositional regimes, ranging from a western, tectonically stable shelf, through platform-ramp to eastern slope and trough-synclines, can be...-
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Published: 01 Feb 2003
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RB 2012/00004 MARREE, South Australia, [geological map] sheet SH54-5. South Australia. Geological Survey. 1:250 000 Series - Explanatory Notes.
The MARREE mapsheet area includes the south-western portion of the Strzelecki Desert plus parts of the Tirari Desert, north-western Flinders Ranges and north-eastern Willouran Ranges, between latitudes 29 to 30 degrees S and longitudes 138 to 139...-
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Published: 01 Apr 2012
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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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ExpNotes MARREE: Explanatory Notes MARREE
A new generation, second edition MARREE 1:250 000 scale geological map and its explanatory notes have been published. These documents represent the conclusion of the Geological Survey of South Australia's latest geological mapping program (1993 to...-
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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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