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RB 84/00020 Jurassic and Permian microfloral assemblages from Weena no. 1 well, southern Cooper Basin.
4 shale samples from 1299 metres to 1307 metres are probably late Early Jurassic to early Middle Jurassic age, (?Hutton Sandstone). Carbonaceous shale from 1526 metres produced an Early Permian microflora characteristic of Stage 3, possibly lower...-
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Published: 01 Mar 1984
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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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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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Stratigraphic cross sections through the Pedirka region.
A collection of 5 stratigraphic cross-sections through the Pedirka region of South Australia, the Northern Territory and Queensland, at a vertical scale of 1:200. GR and sonic well log correlations are related to geological time intervals, utilizing...-
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Palynological examination of core samples from Pandieburra 1, Poonarunna 1, Witcherrie 1, Mokari 1 and Putamurdie 1, western Eromanga Basin, South Australia (MINAD palynological report no. 13/105).
Five core samples from each of Putamurdie No. 1 and Pandieburra No. 1, two core samples from each of Mokarie No. 1 and Witcherrie No. 1 and ten core samples from Poonarunna No. 1 were submitted for palynological examination. The biostratigraphic...-
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Published: 01 Jan 1978
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Synthesis of recent palynological source rock data, PELs 5 and 6 and ATP 259P.
Report discusses the contribution that palynological examination by transmitted and reflected light microscopy can make, alone or in conjunction with geochemical methods, towards characterising the maturity, amount and type of organic matter in a...-
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PEL 5 and PEL 6 biostratigraphic studies. Reports.
There is no abstract created for this record-
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