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- W2393148882 abstract "Salgan and Yingan Shales in Keping region,the source rocks of middle and upper Ordovician in Tarim Basin,northwestern China,were characterized by very low quantities of free biomarkers in traditional Soxhlet extracts,and general steranes and hopanes cannot be detected even in the SIM mode,which makes it difficult to find out the usual oil and source rock correlation.Thus,catalytic hydropyrolysis for kerogens of these source rocks was conducted in order to explore more geochemical information.The results illustrated that little kerogen could display enough and complete biomarker information,which is contributed by high energy at high temperature,protection from H 2 and catalysis from MoS 2,as well as protection supplied by kerogen grid structure.High maturity and magmatic hydrothermal influence were not responsible for the low quantities of free biomarkers.The Keping region in the Ordovician period belongs to platform edge slope and restricted-blocking gulf fancies or deep water shelf-basin face.This special depositional environment is in favor of the input of acritarchs and other related materials but not in favor of the rest biological inputs.As a result,little free biomarkers could be detected in conventional Sohxlet extracts for related acritarchs parent materials." @default.
- W2393148882 created "2016-06-24" @default.
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- W2393148882 date "2012-01-01" @default.
- W2393148882 modified "2023-10-02" @default.
- W2393148882 title "Catalytic hydropyrolysis for kerogens of middle and upper Ordovician source rocks in Keping Section,Tarim Basin,Northwestern China" @default.
- W2393148882 hasPublicationYear "2012" @default.
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