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RB 91/00041 Geology of the KINGOONYA 1:250 000 map sheet area.
Extensive field geological mapping, augmented by petrological and geochemical studies, reinterpretation of company drilling and water-bore logs and a nine-hole drilling programme has detailed the geology of the KINGOONYA area. The stratigraphy spans...-
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Published: 01 Apr 1991
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RB 93/00010 Explanatory Notes for the WARRINA 1:250 000 geological map.
The oldest rocks on WARRINA outcrop in the Peake and Denison Inliers, which comprise the Davenport and Denison Ranges and small inliers to the east. Basement in this area consists of Palaeoproterozoic metamorphic rocks which were intruded by...-
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Published: 01 Jun 1994
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RB 90/00014 Explanatory Notes for the TALLARINGA 1:250 000 geological map.
There is no abstract created for this record-
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Published: 01 Mar 1991
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Wilkinson Lakes East. Annual reports plus final report to licence full surrender, for the period 3/5/2010 to 6/2/2015.
An area centred ~150 km west of Coober Pedy, that is located mostly north-west of and that also has a small part lying immediately south-east of the Karari Fault, a major crustal structure which has controlled deposition at the southern limit of the...-
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Geology and hydrocarbon prospects of the Arckaringa Block.
Due to its thin sequence and shallow depth of burial, most of the Arckaringa Basin is predicted to be immature for hydrocarbon generation in traditional terms. Source rock and vitrinite studies in the Boorthanna Trough however indicate that the basal...-
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Pedirka Sector: a reassessment of geology, porosity, maturity and maturity history.
A review of the Permo-Triassic and Mesozoic distribution of reservoir units. Data for some Birdsville Track Ridge wells are included as the development of the Pedirka Sector basins and the Birdsville Track Ridge are closely related.-
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Arckaringa Block. Farmout block progress reports from November 1982 to January 1989.
Exploration from 1982 includes: Christmas Creek - ARC Seismic Survey (see Envs 4808 and 5064),. Hogarth - ARC Seismic Survey, . Morphett - ARC Seismic Survey,. drilling of 2 wells (Birribiana 1 and Hans Knob 1), (see Envs 7034/6 and 7043/6)....-
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Published: 01 Jan 1989
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Distribution of Permian sediments in the eastern Officer Basin, SA.
The purpose of this study was to determine the extent, thickness and facies of the Permian Arckaringa Basin where it overlies the Officer basin in central northern South Australia. Marine sediments provide important data for sea level curves, and...-
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Organic petrology of samples from a selected group of wells in or near the Arckaringa Block.
34 selected drill core and cuttings samples from six wells were assessed by petrographic methods for their degree of organic maturation and petroleum source potential. The sampled sequence ranged in age from ?Devonian through to Permian, Jurassic and...-
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Billa Kalina Homestead. Progress reports and final report to licence full surrender, for the period 30/6/1977 to 14/2/1979.
Airborne and ground geophysical surveys were undertaken in the Billa Kalina area, prior to commencing to drill in a search for Olympic Dam type Cu-U-Au mineralised haematitic breccias, in order to delineate and detail several broad magnetic anomalies...-
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Bulgunnia. Progress reports and final report to licence full surrender, for the period 22/5/1978 to 10/8/1981.
The base metal and uranium potential of a concealed Proterozoic basement high near Bulgunnia Homestead was evaluated using geological and hydrogeochemical reconnaissance and regional geophysical interpretation approaches. Seismic, ground magnetic and...-
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Reedy Lagoon. Progress reports and final report to licence expiry/full surrender, for the period 3/2/1987 to 2/2/1992.
TARGET: Possible diamondiferous kimberlites subcropping under Cainozoic cover in an area located 110 km north-east of Glendambo. EXPLORATION: Acquisition and interpretation of 6759 line km of airborne magnetic and radiometric surveys, regolith heavy...-
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RB 2006/00001 Guide to the sedimentary cover of the central Gawler Craton, South Australia
The central Gawler Craton is blanketed by thin sedimentary cover that ranges in age from Neoproterozoic to Quaternary. Locally, though, such cover can reach a maximum of ~500 m thickness in Permian glacial valleys or rift structures. This guide...-
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Published: 01 Jan 2006
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RB 2020/00012 Gawler Craton Airborne Geophysical Survey Region 8A, Coober Pedy West – Enhanced geophysical imagery and magnetic source depth models
This report presents the results of a study jointly conducted by the Geological Survey of South Australia and CSIRO Mineral Resources which aimed to enhance the expression of geological structure in geophysical images and to derive depth to magnetic...-
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Published: 01 Apr 2020
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Reedy Lagoon. Progress and final reports to licence surrender for the period 20/7/81 to 4/8/86.
Exploration as part of a continuing regional search for possible diamondiferous kimberlites was undertaken 70 km west-northwest of Roxby Downs. Extensive sampling of current drainage lines in interdune swales, plus loam sampling in other...-
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Mount Woods. Combined first progress/final report at licence full surrender, for the period 6/9/1979 to 5/12/1979.
Following an evaluation of existing subsurface data, 9 vertical percussion holes totalling 670 m were drilled to test discrete gravity anomalies in the Mount Woods area, in a search for Olympic Dam type mineralisation. The holes encountered...-
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ExpNotes BARTON: Explanatory Notes BARTON, SH 53-09.
Shallow Precambrian crystalline basement underlies the greater part of the BARTON 1:250 000 map area. Thicker Neoproterozoic, Cambrian and Carboniferous Permian sediments occur in the northwest, with the southern margin bounded by the Karari Fault...-
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ExpNotes COOBER PEDY: Explanatory Notes COOBER PEDY, SH 53-06.
There is no abstract created for this record.-
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ExpNotes GILES: Explanatory Notes GILES, SH 53-01.
Concealed basement on GILES comprises ?Archaean to Palaeoproterozoic metamorphic rocks belonging to the Nawa Subdomain of the Gawler Craton. These are intruded by Mesoproterozoic Hiltaba Suite granitic bodies and Mesoproterozoic or Neoproterozoic...-
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