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Rachel Robinson

Researcher at Geological Survey of Canada

Publications -  9
Citations -  186

Rachel Robinson is an academic researcher from Geological Survey of Canada. The author has contributed to research in topics: Source rock & Hydrocarbon. The author has an hindex of 5, co-authored 7 publications receiving 148 citations.

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Hydrocarbon evaporative loss from shale core samples as revealed by Rock-Eval and thermal desorption-gas chromatography analysis: Its geochemical and geological implications

TL;DR: In this article, a time-series of Rock-Eval and thermal desorption-gas chromatography (TD-GC) analyses have been carried out on an organic-rich Devonian Duvernay Formation shale core sample from the Western Canada Sedimentary Basin (WCSB) and an organiclean Ordovician Lotbiniere Formation (Lotbiniere) core sample, which still contains high relative concentrations of C7-C9 hydrocarbons.
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Organic geochemistry and organic petrology of a potential source rock of early Eocene age in the Beaufort–Mackenzie Basin

TL;DR: The biological marker compounds 17α(H) and 17β(H), 23,28-bisnorlupane have been identified in a coaly interval at about 3300-3320 m depth within the lower Taglu Sequence (early Eocene) in the Immiugak A-06 well in the Beaufort-Mackenzie Basin this article.
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Chemical and petrographic evidence for thermal cracking and thermochemical sulfate reduction of paleo-oil accumulations in the NE Sichuan Basin, China

TL;DR: In this article, an integrated chemical and petrographic approach for distinguishing solid bitumens formed by thermal cracking and by thermochemical sulfate reduction (TSR) was presented, which suggests that sulfate supply appears to be a major limiting factor for the TSR reactions involving gaseous alkanes.
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Two-dimensional gas chromatograms as fingerprints of sour gas-associated oils

TL;DR: In this article, a well-documented case history in Western Canada sedimentary basin using two-dimensional gas chromatography has produced a useful tool for fingerprinting thermochemical sulfate reduction (TSR)-affected petroleum fluids.
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Organic petrographic analysis of artificially matured chitinozoan- and graptolite-rich Upper Ordovician shale from Hudson Bay Basin, Canada

TL;DR: In this paper, the degree of physicochemical transformation of dispersed organic matter (DOM) and zooclasts in BRF petroleum source rock after artificial maturation was quantitatively and quantitatively assessed, and the relationship between graptolite, chitinozoan, vitrinite-like particle and bitumen reflectance was determined with increasing pyrolysis temperature and the thermal maturity.