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RB 79/00092 Petrophysical data on Wilkinson stratigraphic drillhole no. 1.
Various petrophysical property measurements (total count radiometric, mag susceptibility and specific gravity) were made at 1-metre intervals on samples of stored drill core recovered from the hole depth range 210 m to 710 m (TD) in SADME Wilkinson 1...-
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Published: 01 Jul 1983
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RB 80/00005 Source book for the Officer Basin area in South Australia.
This is a bibliographic compilation with index and key maps on petroleum potential, geology, geophysics and palaeontology of the Proterozoic-Palaeozoic Officer Basin, post-Palaeozoic geology, tectonics and other related topics.-
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Published: 01 Feb 1980
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RB 77/00053 Murnaroo 1. Micropalaeontological investigation.
There is no abstract created for this record-
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Published: 01 Jan 1977
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RB 79/00088 Wilkinson 1. Well completion report.
Wilkinson 1 stratigraphic well was drilled by the SA Department of Mines and Energy in mid-1978, about 250 km south-west of Coober Pedy, in the Tallaringa Trough. Here a thick section of Cambrian claystones, limestones and evaporites, at least 594 m...-
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Published: 01 Oct 1979
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RB 80/00010 Oil geochemistry and assessment of hydrocarbon source potential of Cambrian and Devonian rocks, Officer Basin, South Australia.
Oil shows in the Observatory Hill Beds in Byilkaoora 1 occur in a non-marine, alkaline playa lake sequence. Geochemical analysis suggests that they are immature and belong to 2 primary genetic families. The less altered oils are quite unlike...-
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Published: 01 May 1980
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RB 97/00056 An assessment of the groundwater resources of the Lake Maurice area, northwest South Australia, for the Oak Valley Community, Maralinga Tjarutja Aboriginal Lands.
The Oak Valley Community requires a more convenient water supply. If potable groundwater cannot be found then a supply suitable for purification must be found. Current requirements are a supply of 1 L/s of water of salinity not greater than 40 000...-
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Published: 01 Dec 1997
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RB 99/00031 Assessment of zinc-lead prospectivity on the Murnaroo Platform and in the Manya Trough, eastern Officer Basin, South Australia.
The Neoproterozoic to Palaeozoic Officer Basin is located on and adjacent to the northwestern margin of the Gawler Craton. Deposition of the basin began in Adelaidean time, before and during the breakup of the supercontinent Rodinia. The...-
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Published: 01 Dec 1999
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RB 89/00006 GILES, TALLARINGA and BARTON 1:250 000 sheet. Water well survey.
Of 124 wells visited, salinity was measured from 41 wells and 95 wells which were not located were added to the Bore General File. Groundwater used for stock and domestic purposes ranges in salinity from 400 ppm to 25 000 ppm. Other wells have...-
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Published: 01 Feb 1989
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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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RB 95/00011 Hydrocarbon shows in Comalco mineral drillholes, Officer Basin.
The Officer Basin covers some 350,000 square km of central southern Australia, extending from the Yilgarn Block in Western Australia east to the Gawler Craton in South Australia. During the early 1980s Comalco Aluminium Limited explored the eastern...-
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Published: 01 Mar 1995
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Wilkinson. Annual reports plus final report to licence expiry/full surrender, for the period 4/1/1999 to 3/1/2002.
Possible potash and halite resources in evaporite - rich sediment sequences of the Tallaringa Trough, lying at depths that might be suitable for solution mining, were the initial targets of exploration in the Wilkinson Lakes area. Following a...-
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Evaporites in the Officer Basin.
The Officer Basin covers about 300,000 square km and is largely concealed beneath sediments of the Gibson and Great Victoria deserts in western and southern Australia. Approximately two-thirds of the Officer Basin lies in Western Australia....-
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Published: 07 Jan 1998
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Wintinna Hill, Welbourn Hill Homestead, South Neales River and Mount Willoughby Homestead. Joint progress reports to licences' joint full surrender, for the period 11/11/1986 to 10/11/1987.
An extensive review was undertaken of the potential of the eastern Officer Basin area extending 50-150 km west of Oodnadatta for hosting buried native sulphur deposits in association with salt dome structures, but the recommended follow-up exploration...-
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Published: 20 Jan 1988
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Burial history analysis of the east Officer Basin, South Australia. A preliminary study.
In South Australia, the intracratonic eastern Officer Basin, which may contain up to 10 km of Neoproterozoic to Paleozoic sediments, is bounded by the Precambrian Gawler Craton to the southeast, the Musgrave Block to the north, and passes into...-
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Eastern Officer Basin technical assessment.
This technical assessment of petroleum prospectivity and attendant exploration risk for the eastern Officer Basin was prepared by SAOGC staff to help management decide the merits or otherwise of making a PEL application for vacant acreage gazetted by...-
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Byilkaoora 1. Test reports.
Contains various detailed source rock analysis reports on drill core samples from the oil-bearing interval in the well.-
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Published: 17 Jun 1981
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PEL 30. Progress reports from 12/2/85 to 12/2/88.
Exploration for sodium carbonate, base metals and petroleum included detailed logging and sampling of Byilkaoora 2, seismic survey (76 km of 60 fold Vibroseis data recorded at 30 metre intervals), and drilling and shooting of 10 upholes, geologically...-
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Sedimentology of the Ouldburra Formation (Early Cambrian), northeastern Officer Basin.
The Ouldburra Formation (Early Cambrian) is a newly defined sequence of carbonates, mixed carbonate/siliciclastics and evaporites in the northeastern Officer Basin, northern South Australia. Deposition took place during the late stages of...-
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Exploration of PEL 23 and PEL 30, eastern Officer Basin, South Australia, 1983-1988.
This licence relinquishment report includes a description of regional stratigraphy and summary of exploration seismic interpretation and drilling results. The quality and distribution within (and projected outside of) PELs 23 and 30 of the source...-
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PEL 23. 1983 source rock, geochemistry and porosity / permeability studies.
Rock-eval data for Byilkaoora 2 and 3 do not agree with elemental analytical studies previously carried out on similar rocks in Byilkaoora 1. Biomarker studies will be undertaken in an effort to resolve these difficulties.-
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Published: 01 Jan 1984
