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RB 79/00083 Ooldea no. 1 and Reid nos 1 and 1A. Well completion reports.
Three stratigraphic wells (Ooldea no. 1, Reid no. 1, and Reid no. 1A) were drilled by the South Australian Department of Mines during 1976 in an area that includes margins of the Officer, Arckaringa and Eucla basins. Principal objectives were to test...-
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Published: 01 Jan 1979
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Murrawijinie, Denman, Koonalda and Cook [Wigunda]. Progress and final reports for the period 7/7/80 to 27/7/81.
Cretaceous sediments in the Eucla Basin portion lying within South Australia's far west were investigated for their oil shale potential. This search was prompted by a recorded occurrence of a thick, oily Cretaceous shale horizon intersected in a...-
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Published: 10 Jun 1981
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PEL 33, Eucla and Denman Basins. Progress reports for the period 25/6/85 to 18/4/89.
Contains interpretation reports on satellite imagery remote sensing and reprocessed aeromagnetic data, plus other brief interpretative statements by the contract operator contained within some quarterly tenement reports.-
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Published: 18 Apr 1989
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1987 seismic surveys, Denman and Denman 'B', final reports.
Denman Seismic Survey - AIM: This seismic survey of 4 lines totalling 40.0 line kms coverage was conducted in the southern Denman Trough, in the vicinity of Outback Oil's Denman 1 well drilled in 1966, in order to fulfil the Licence Year 2 work...-
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Eucla Basin Stratigraphic Drilling Project. Well completion reports.
Four wells, drilled within 36 km of the Hughes and Denman Railway Sidings, explored for a possible Palaeozoic section and/or Upper Proterozoic or older basement, that was expected from Outback's regional gravity survey data to occur at or around...-
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RB 00780 Brief study of the Eucla Basin, with recommendations for further petroleum work.
This report provides a brief summary of the geology and petroleum potential of the onshore, South Australian portion of the Eucla Basin at the time of termination of PEL 4, with the aim of providing a starting point for more thorough studies.-
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Published: 31 Jan 1900
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RB 00843 Geology of the Maralinga area, South Australia.
Maralinga is located on the crest of the Ooldea Range, an ancient (Tertiary) coastal dune which is bounded to the south by the Nullarbor Plain and to the north by Tietkens Plain. The dune field of the Great Victoria Desert covers much of the region...-
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RB 00731 Hughes-Denman Stratigraphic Drilling Project of Outback Oil Company NL. Subsurface stratigraphy and micropalaeontological study and Outback Oil Hughes and Denman wells. Palynological report.
The four stratigraphic wells completed in the Eucla Basin within 20 miles of the Hughes and Denman Railway Sidings intersected a sequence of Tertiary, Lower Cretaceous, probable Palaeozoic, and possibly some Proterozoic rocks. The ages of the...-
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Published: 01 Nov 1900
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RB 71/00004 Comments on NOORINA, WYOLA, MAURICE 1:250 000 geological sheets.
Preliminary maps were compiled by photointerpretation with limited geological ground control. Some topographic features and photo - lineaments are considered structurally significant and may reflect faults with NE - ENE and NW orientations. The...-
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Published: 11 Jan 1971
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RB 2007/00011 Original full content version of] OOLDEA, South Australia, [geological map] sheet SH52-12. South Australia. Geological Survey. 1:250 000 Series - Explanatory Notes.
The OOLDEA 1:250 000 map area, in the far west of SA, includes portions of the Maralinga Tjarutja Aboriginal Lands, Maralinga Prohibited Area, and Nullarbor Regional Reserve. It is traversed by the Trans-Australian Railway. There is no significant...-
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Published: 01 Jun 2007
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RB 2022/00011 Eucla Basin and peripheral paleovalleys.
The Cenozoic Eucla Basin is located on the southern margin of the Australian continent, with a present-day basin onshore edge which extends for over 2,000 km from Western Australia into South Australia. The basin’s sediment fill comprises a thin...-
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Published: 01 Nov 2022
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ExpNotes OOLDEA: Explanatory Notes OOLDEA
There is no abstract created for this record-
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ExpNotes BARTON: Explanatory Notes BARTON
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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