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Report on a gechemical evaluation of the Mokari 1 and Purni 1 wells, Pedirka Basin, South Australia.
4 samples of conventional drillcores from the Lower Permian section in each of Mokari 1 (depth interval 6074.5-6618.5 feet KB) and Purni 1 (depth interval 4742-5810 feet KB) were analysed for source rock geochemistry. Measurements of vitrinite...-
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Purni 1. Test reports.
Contains results of government consultants' palynological and palaeontological studies of drill cuttings and cores, plus data obtained from DST fluid sample water and gas analyses and from conventional core analyses and source rock analytical...-
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Source rock and petroleum geochemistry of the Eringa Trough, Pedirka Basin.
6 drill core samples and 68 drill cuttings samples from selected organic-rich intervals in 4 Eringa Trough wells were subjected to organic geochemical and petrographic analyses to enable assessment of their hydrocarbon generative potential. Following...-
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Source rock and petroleum geochemistry of the Eringa Trough, Pedirka Basin. Supplementary report.
3 drill core samples from the Early Permian in Purni 1 and Witcherrie 1 were analysed for TOC, Rock Eval pyrolysis, petrographic and vitrinite reflectance data to allow a check and comparison with anomalous aromatic hydrocarbon biomarker ratios...-
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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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Macumba 1. Test reports.
There is no abstract created for this record-
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Source rock potential and petroleum geochemistry of the Eringa Trough area, Pedirka Basin.
As part of a MESA-led reappraisal of the source rock potential of the Eringa Trough, Pedirka Basin, this study was commissioned to carry out an organic geochemical and petrographic investigation of coals and carbonaceous sediments from the margins of...-
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