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RB 83/00056 Edeowie 1. Well completion report.
Edeowie 1 (TD 984 metres), which aimed to identify a series of seismic reflectors mapped by SADME beneath the eastern Lake Torrens piedmont plain, has intersected a stratigraphic sequence with features indicating that complex structural changes occur...-
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Published: 01 Jul 1983
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RB 85/00026 Report of a gravity survey over the eastern Arrowie Basin, South Australia.
Survey was located on 7 seismic lines. Gravity interpretation indicates deep basement structure associated with Precambrian sediments. Features within the Tertiary - Cainozoic units are delineated. Further work is recommended to investigate possible...-
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Published: 01 Apr 1986
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RB 93/00021 New overprint from the Delamerian fold belt and the Cambro-Ordovician APWP for Gondwanaland.
A paleomagnetic study of the mid- to Late Cambrian sedimentary rocks in the northern Delamerian fold belt reveals an overprint acquired after regional folding during the Cambro-Ordovician. The paleopole position, based on data from eight sites, is...-
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Published: 01 Apr 1993
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Source rock maturity study, Arrowie Basin, South Australia - Parts I and II.
A small suite of Cambrian rock samples was selected to evaluate the use of the methylphenanthrene index (MPI) and other aromatic hydrocarbon ratios as measures of thermal maturity in Early Palaeozoic sequences. Such very old rocks do not contain woody...-
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Published: 08 Aug 1986
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Source rock maturity study and petroleum geochemistry of the Arrowie Basin.
This section of the study was based on source rock analyses performed on 75 outcrop and shallow drill core samples from 25 localities, plus other new data derived from Cambrian sediments intersected in the deep petroleum exploration wells Moorowie 1,...-
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Published: 13 Jan 1986
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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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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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Wertaloona, Bunyeroo and Coffins Bore. Final report at licences' joint surrender, for the period 1/11/1977 to 23/11/1977.
Three small infrabasins containing Middle Cambrian sediments deposited at the culmination of filling of the Adelaide Geosyncline by sedimentation were explored for possible economic stratiform base metal mineralisation. Work comprised the field...-
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Published: 18 Sep 1978
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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 71/00035 PARACHILNA, South Australia, sheet SH54-13 International Index.
The Parachilna 1:250 000 map area is about 250 road miles north of Adelaide, South Australia, and includes the eastern shore of Lake Torrens, the central Flinders Ranges and part of the Lake Frome Plains. The ranges are composed of folded Adelaidean...-
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Published: 01 Jan 1972
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Teatree Well. Progress and final reports to licence expiry/full surrender for the period 5/1/1984 to 4/1/1986.
Exploration for possible fault-related epigenetic lead-zinc deposits formed in calcareous rocks outcropping along the Mount John - Arrowie fault system, to the south-east of the Moro mine, has included extensive stream sediment and rock chip sampling...-
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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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