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- W2354484892 abstract "In combination with the geological background and sedimentary evolution in the eastern Sichuan Basin,the data of illite crystallinity,vitrinite reflectance(VR o),bitumen reflectance(BR o)and homogenization temperature of fluid inclusions of Mesozoic-Paleozoic core(debris) samples show that Mesozoic continental strata in eastern Sichuan Basin are characterized with illite crystallinity values over 0.42°(Δ2θ),the VR o and BR o less than 3%,and lies in late diagenetic stage.Mesozoic-Paleozoic marine strata are characterized with illite crystallinity values from 0.25 to 0.42°(Δ2θ),the VR o and BR o from 3% to 6.5%,and lies in very low-grade metamorphic stage.The value of illite crystallinity has a good linear relation with homogenization temperature of fluid inclusions and the paleotemperature deduced from VR o.While the value of illite crystallinity is equal to 0.42°(Δ2θ),the paleotemperature and homogenization temperature of inclusions are about 180℃.The illite crystallinity value is an indicator of important thermal maturity and paleotemperature at the digenetic-metamorphic and high-over mature stages." @default.
- W2354484892 created "2016-06-24" @default.
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- W2354484892 date "2009-01-01" @default.
- W2354484892 modified "2023-09-25" @default.
- W2354484892 title "Research on maturity indicators of high-maturity marine strata in the eastern Sichuan Basin" @default.
- W2354484892 hasPublicationYear "2009" @default.
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