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RB 82/00072 Organic carbon and trace element investigations, Cooper Basin sediments. Fifth progress report - Carbon distribution.
Carbonate carbon and to a lesser extent organic carbon are persistent in their pattern of vertical distribution regardless of structural position. Detailed correlations may be made across the SE of the basin. Idealised chemostratigraphic successions...-
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Published: 01 Nov 1982
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Organic petrology of a suite of samples from Merrimelia 15 and a comparison with Merrimelia 6 and 7.
Ten samples of drill cuttings from Merrimelia 15 were examined in polished section under normally incident white light and under reflected light UV fluorescence mode. Brief descriptions of the dispersed organic matter contained in each sample, plus...-
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Crude oil characterisation and correlation study of twenty crude oils from the Cooper-Eromanga Basin, South Australia.
Organic geochemical analyses of 20 crude oil samples from twelve wells were performed to determine if any genetic oil families could be identified within the Eromanga-Cooper Basin area. The results have been plotted graphically to demonstrate the...-
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Crude oil to parent source rock correlation study, Wancoocha Field.
Organic geochemical analyses were performed on 14 conventional core samples taken from the Epsilon, Murteree and Patchawarra formation intervals in Wancoocha 1 and on 3 similar samples from the Birkhead Formation in Wancoocha 4. The rock sample...-
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Novel approaches to the determination of the origins of petroleum hydrocarbons in the Cooper-Eromanga Basin system.
In June 1996 MESA commissioned the Centre for Petroleum and Environmental Organic Geochemistry at Curtin University with $30 000 to investigate the applications to the Cooper-Eromanga Basin system of new molecular geochemical concepts recently...-
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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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Vitrinite reflectance data from the Cooper and Eromanga Basins.
The vitrinite reflectance technique is considered by the PELs 5 and 6 and ATP259P licensees to be the most reliable means of measuring the maturity of a sedimentary sequence. This subject suite of isoreflectance maps was prepared using vitrinite...-
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Results of rock-evaluation pyrolysis measurements carried out on selected drill cuttings and core samples from 9 Patchawarra Trough wells.
There is no abstract created for this record-
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Published: 30 Jul 1986
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Hydrologic constraints on petroleum generation and migration within the Cooper and Eromanga Basins, South Australia. CSIRO / University of New Hampshire, USA, collaborative study. Project initiation and progress reports.
The Cooper and Eromanga Basins region, Australia's most productive onshore petroleum province, has a regional groundwater flow system over 1500 km in length. While the present-day hydrology of the Cretaceous and Jurassic aquifer system is well...-
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Published: 02 Oct 1992
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Liquid chromatography data available in PELs 5 and 6 and ATP 259P.
This report synthesises all existing Delhi-Santos' Cooper Basin area Mesozoic and Permian petroleum source rock geochemical data relating to liquid chromatography, providing a basis for further source rock work to be carried out on a...-
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Merrimelia-Innamincka Farmout Block reports.
There is no abstract created for this record-
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Crude oil characterisation and correlation study, twenty-seven oils, South Australia-Queensland Cooper-Eromanga Basin.
27 oil samples obtained on drillstem testing of various Mesozoic and Permian formations in wells spread across the Delhi-Santos petroleum exploration licence areas were subjected to organic geochemical analysis to determine their geochemical...-
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Crude oil characterisation of six crude oils from the Eromanga-Cooper Basin(s), South Australia.
The following organic geochemical analyses were performed on 6 oil samples produced from five different Cretaceous to Permian age reservoirs in 4 wells drilled by Delhi Petroleum: 1) C1-C31 whole oil gas-liquid chromatography; 2) C4-C7 gasoline...-
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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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Notes on the regional play maps for the Cooper Sector (of PELs 5 and 6) and ATP 259P.
This report presents a set of tenement-based petroleum exploration play maps synthesizing the licensees' accumulated hydrocarbon discovery, seal, porosity, source and maturity data for the major reservoirs in the Cooper and Eromanga Basins, viz. the...-
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Vitrinite reflectance profiles and iso-maturity maps of the Cooper-Eromanga Basin.
There is no abstract created for this record-
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Crude oil - Parent source rock evaluation study, Murta Block, Cooper-Eromanga Basin(s), South Australia.
The following organic geochemical analyses were performed on 7 sidewall core and 4 crude oil samples from Wancoocha 2, 1 crude oil sample from Wancoocha 3 and 1 crude oil sample from Pando 1: 1) C1-C31 whole oil gas-liquid chromatography; 2) C4-C7...-
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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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ExpNotes CALLABONNA: Explanatory Notes CALLABONNA
There is no abstract created for this record-
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ExpNotes STRZELECKI: Explanatory Notes STRZELECKI
The STRZELECKI 1:250 000 map area lies adjacent to the NSW border in the centre of the Strzelecki Desert, and covers some of the main hydrocarbon producing areas in SA around Moomba. Most of these oil and gas fields are located in the northern half of...-
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