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SCI周文-Differential fluid migration behaviour and tectonic movement in Lower Silurian and Lower Cambr
发布时间:2018-08-14   作者:admin

Isotope geochemistry has been introduced as a means to trace origin of the hydrocarbon and characterize highly productive shale gas systems recently. To assess the impact of tectonic movement and the sealing of shale gas systems, isotope geochemistry, pressure coefficients and the distribution of bitumens are analysed. Many samples yield isotope geochemical data with typical carbon isotopic reversals (d13C1 > d13C2) and hydrogen isotopic reversals (d13DC2H6 > d13DCH4) in the Lower Silu



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