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Hydrocarbon potential of the Jurassic and Lower Cretaceous sediments from five wells in the Eromanga Basin, South Australia.
Organic matter in Jurassic and lower Cretaceous sediments from 5 wells in the central Eromanga Basin was studied microscopically. The lower Jurassic Birkhead Formation, upper Jurassic to lower Cretaceous Murta Member and lower Cretaceous Transition...-
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Eromanga Basin source rock studies. Reports.
There is no abstract created for this record-
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Hydrocarbon potential and environmental interpretations of the Jurassic - Lower Cretaceous section in five wells in the Eromanga Basin.
Five wells along a north-south trending section in the southern Eromanga Basin were studied using petrographic techniques to delineate petroleum source rocks and possibly aid in environmental interpretation. The dispersed organic matter (d.o.m.) in...-
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Pedirka Block. Acreage assessment report.
An assessment of the petroleum potential of the Pedirka farmout area, occasioned by the February 1989 compulsory 25% acreage relinquishment of PELs 5 and 6. Items reviewed include Block geology, farmout arrangements, future commitments, an inventory...-
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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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PEL 50, Tirari Desert. Progress and technical reports for the period 1/7/91 to 30/6/2001.
There is no abstract created for this record-
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Apatite fission track analysis of samples from the western Eromanga Basin and Eringa Trough, Australia.
16 rock samples from wells and outcrop in the western Eromanga Basin / Eringa Trough region were analysed for their apatite grain fission track properties to derive an interpretation of the geothermal history of the enclosing strata.-
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PEL 50, Eromanga Basin, South Australia. Farm-out brochure and supporting data.
Petroleum Exploration Licence 50 in northern South Australia covers approximately 9714 square km of the prospective Eromanga Basin, in which over 400 million barrels of oil in place have been discovered since 1977. To date, only 3 exploratory wells...-
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Source rock richness in the Eromanga and Cooper Basins. Total organic carbon (TOC) data.
A study of source-rock richness has entailed the evaluation of TOC data for the Eromanga and Cooper Basins. TOC analyses were averaged and plotted on 1:250 000 basemaps, on a formation by formation basis. The data were contoured by honouring all data...-
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Progressive report on the PhD research project entitled: Source rock and petroleum geochemistry of the Poolowanna Formation (basal Jurassic), Eromanga Basin.
This report describes the work performed during the first year of a 3-year PhD research project, which commenced on 24/2/93. To start with the author carried out a literature review of previous work on petroleum geochemistry in the Cooper and Eromanga...-
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Organic petrology of the Birkhead Formation, Eromanga Basin (continued).
Drill cuttings samples of the Birkhead Formation from a further 16 wells to those originally sampled were selected for a petrographic study of the organic matter they contain. Comparisons were made between the organic petrographic characteristics of...-
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Preliminary evaluation of Eromanga Basin seals (Oil Project 88-12).
Primary regional seals for Eromanga Basin oil reservoirs in the Cooper Sector of PELs 5 and 6 are the Birkhead Formation and the basal part of the Murta Member. Intra-formational seals occur locally within the Poolowanna, Birkhead and Westbourne...-
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Published: 27 Oct 1988
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Organic petrology of the Birkhead Formation, Eromanga Basin.
Drill cuttings samples of the Birkhead Formation from 16 wells were selected for a petrographic study of the organic matter they contain. Comparisons were made between the organic petrographic characteristics of wells with no shows in either the...-
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Petroleum exploration review, PEL 55, Eromanga Basin, South Australia.
This report examines the prospectivity of PEL 55 in considerable detail, in order to construct a dataset suitable for attracting new farminees so that outstanding drilling work on the licence may be progressed. The favourable setting of the licence...-
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Source rock and petroleum geochemistry of the Simpson [Desert] Basin and superjacent western Eromanga Basin (Pandieburra 1, Poonarunna 1, Putamurdie 1).
This is the final in a series of reports prepared for MESA, in which the hydrocarbon source potential of the Pedirka, Simpson and western Eromanga Basins is re-evaluated. Previous work focused on the Eringa Trough of the Pedirka Basin and the...-
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MESA Pedirka and Eromanga Basins Thermal and Tectonic History Project. Reports for the period January 1995 to December 1996.
Apatite fission track analysis (AFTA), detailed source rock property and organic maceral vitrinite reflectance data has been collected from several key wells neighbouring the Eringa Trough, as part of a collaborative ARC grant project run by MESA and...-
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PEL 49, Simpson Desert. Progress and technical reports for the period 1/7/91 to 30/6/2001.
There is no abstract created for this record-
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Block prospectivity summary, Birdsville Track Ridge Block, February 1983.
The Birdsville Track Ridge (BTR) Block is dominated by a large, low relief Cambro-Ordovician basement' ridge which trends NNE-SSW through the block. Permian sediments onlap the eastern flank of the ridge, but only extend into the easternmost part of...-
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Regional isopach maps of the Jurassic sequence in the Eromanga Basin. A preliminary approach.
Report discusses the compilation and interpretation of 5 isopach maps prepared to illustrate spatial and temporal patterns of regional structural growth history in the Eromanga Basin sequence. The maps also provide a basis for predicting regional...-
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Source potential of the Eromanga Basin sequence, Patchawarra Trough area (Oil Project 88-11).
A number of oil recoveries have been made, and oil shows recorded, around the margins of the Patchawarra Trough. The bulk of this oil is generally believed to be derived from the Cooper Basin, with transmission to the Eromanga section where the...-
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