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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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1970 seismic and gravity survey, Frome Downs, final report.
Comprises details of the operations, field acquisition, results and interpretation of the seismic and gravity survey. A total of 2324 profiles covering 555 miles were recorded; 1584 gravity stations were metered. The survey aimed to locate prospective...-
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Published: 01 Jan 1971
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1981 and 1982 seismic surveys, Wertaloona and Christmas Creek-ARR, final report.
Wertaloona Seismic Survey - AIM:The 1981 Wertaloona Seismic Survey programme was designed by the PELs 5 and 6 Arrowie Block partners to provide the first high quality, multifold seismic reflection data in the area of likely preserved thick Cambrian...-
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Frome Downs seismic and gravity survey. Progress reports March 1970 - March 1971.
There is no abstract created for this record-
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Published: 01 Jan 1971
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Arrowie Block acreage assessment.
During the period January 1946-December 1985 under review, the following petroleum exploration work was carried out over the Arrowie Block: 6 gravity, 2 aeromagnetic and 10 seismic surveys (total seismic coverage 2781 line km), plus 4 wells, all dry....-
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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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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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