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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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1982 seismic survey, Christmas Creek, final report.
AIM:The 1982 Christmas Creek Seismic Survey was designed to cover a wide area of the sparsely explored western farmout blocks of PELs 5 and 6, where Eromanga Basin sediments thin and overly sub-basins of variously aged prospective sediments. Primary...-
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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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Organic petrology of samples from a selected group of wells in or near the Arckaringa Block.
Nineteen drill cuttings and 15 drill core samples of Permian, Cretaceous and Jurassic ages were assessed for organic maturation and source rock potential.-
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Geology of the Arckaringa Basin, South Australia.
A description of the overall structure and stratigraphy of the Basin and identification of areas for potential coal development, based on all open file information.-
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RB 73/00098 A Synthesis of Stratigraphic drilling in the Arckaringa Basin, 1969-1971.
The SA Department of Mines drilled seven stratigraphic wells between 1969 and 1971 in the Arckaringa Basin. This study presents the stratigraphic information obtained and attempts to collate all available information in a synthesis of the Arckaringa...-
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Published: 01 Jan 1976
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RB 75/00015 Revision of Permian and Devonian nomenclature of four formations in and below the Arckaringa Basin.
There is no abstract created for this record-
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Published: 31 Jan 1975
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Mount Sarah Homestead. Annual reports to licence expiry/renewal, for the period 24/5/2002 to 23/5/2007.
An area located approximately 75 km north-west of Oodnadatta is being explored for possible economic sedex style or MVT base metal sulphides that could have formed in Permian and early Cambrian sediments, and for any Proterozoic basement-hosted IOCG...-
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