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Formations of the Gidgealpa Group in the Cooper Basin.
A sedimentary sequence of Permian age provides both the source and reservoirs for the major portion of the hydrocarbons discovered in the Cooper Basin. This sequence is composed of shales, siltstones, coals and sandstones, and in 1967 was named the...-
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1979 Moonlight Flat Seismic Survey. Final report.
AIM: To mature several large structural leads, map possible stratigraphic traps on the flanks of regional highs and extend the regional Vibroseis coverage. METHODS: Survey dates: 10/4/79 - 23/11/79. Energy source: Vibroseis. CDP coverage: 1200%....-
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1978 seismic survey, Perigundi, final report.
AIM:The 1978 Perigundi Seismic Survey was the fourth modern, digital Vibroseis survey conducted in the Cooper Basin, and was based on similar concepts to the 1973 Mudlankie, 1975 Tooroopie and 1976 Callamurra regional surveys, namely: 1) to further...-
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Table of Permian formation tops, Cooper Basin wells, to August 1972.
There is no abstract created for this record-
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Epsilon area stratigraphic study (of) the Gidgealpa Group in the Cooper Basin.
Permian stratigraphy in the southeastern portion of the Cooper Basin has been studied by the licensees to further their understanding of its depositional environments and to attempt to establish depositional trends. If relationships between...-
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Cooper Basin stratigraphy. Reports for the period June to November 1972.
There is no abstract created for this record-
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1973 seismic survey, Mudlankie, final report.
AIM: The Mudlankie Seismic Survey was the first extensive survey using the Vibroseis method to be carried out over a wide area of the southwestern Cooper Basin, and was designed: (1) to augment the mapping of existing fields and improve their...-
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Published: 01 Jan 1974
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RI 043 The Hydrology of the Gidgealpa Formation of the Western And Central Cooper Basin
A study of the chemical aspects of Permian and Mesozoic formation waters has enabled the zones of flushing of Permian sediments by artesian waters to be clearly delineated. It has been proved that complete flushing has taken place in the southern...-
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Rank variation in the Cooper and Eromanga Basins, central Australia.
The Cooper Basin is an infra-basin (area 127 000 km2) containing a Permian to Triassic age succession which is overlain by Jurassic and Cretaceous age sedimentary rocks of the Eromanga Basin. Coal beds occur throughout the entire section. Oil and...-
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Bull 049 Regional Stratigraphic Analysis of the Gidgealpa Group, Southern Cooper Basin, Australia
A regional stratigraphic analysis, using mainly quantitative data derived from wireline logs, has led to the reconstruction of the palaeogeography and depositional history of the Permian Gidgealpa Group within the southern Cooper Basin. The Cooper...-
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RB 00768 Hydrology of the Gidgealpa Formation of the western and central Cooper Basin.
A study of the chemical aspects of Permian and Mesozoic formation waters has enabled the zones of flushing of Permian sediments by artesian waters to be clearly delineated. It has been proved that complete flushing has taken place in the southern...-
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Published: 01 Dec 1900
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RB 00759 Basin study of [sub-basins to] the Great Artesian Basin, South Australia: Palaeozoic and Triassic [sediments].
Report discusses via a series of maps the subsurface geology of the Cooper and Pedirka regions underlying the Great Artesian Basin in South Australia. A general tectonic and depositional environmental framework is delineated for each of 3 layers of...-
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Published: 31 Dec 1899
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RB 74/00217 Explanatory Notes for the INNAMINCKA 1:250 000 geological map.
The INNAMINCKA 1:250 000 map area is located in the north-east of the state, adjacent to the SA-Queensland state border. It lies between latitudes 27°00 and 28°00 and longitudes 139°30' and 141°00. It is one of the best explored areas of the state in...-
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Published: 02 Dec 1974
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RB 98/00024 Cooper Basin Folio. Summary Report and Volume 1 seismic maps and Volume 2 geological maps (updated version).
This folio is the culmination of an extensive seismic mapping and interpretation of the Cooper and Eromanga Basins, South Australia that commenced in 1995. It follows earlier mapping of the C Horizon (Top Cadna-owie Formation) that commenced in 1991....-
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Published: 01 Oct 1998
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RB 2009/00001 Explanatory Notes for [the] CALLABONNA 1:250 000 Geological Map, sheet SH 54-6.
The CALLABONNA map area includes the southern end of the Strzelecki Desert and the north- eastern Flinders Ranges, between latitudes 29° to 30° S and longitudes 139° 30' to 141° E. Cameron Corner adjoins New South Wales and Queensland in the...-
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Published: 01 Oct 2009
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Clay minerals of the Gidgealpa Permian sediments.
12 selected drill core specimens were analysed.-
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ExpNotes CALLABONNA: Explanatory Notes CALLABONNA, SH 54-06.
There is no abstract created for this record.-
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