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- W2357251837 abstract "Based on open and restriction simulation experimental system,the gas-generation process and evolvement condition of methane carbon isotope of deep hydrocarbon source rocks in Xujiaweizi fault depression were quantitatively evaluated by using hydrocarbon-generation and methane carbon isotope kinetic methods combined with heat and burial history.The results show that the source rocks of Shahezi Formation began to generate gases at the time of Denglouku Formation.The gas-generation peak period is from Quantou Formation to Qingshankou Formation.The gas-generation threshold depths of mudstone and coal are nearly 2 100 m and 1 750 m,corresponding to the vitrinite reflectance of 0.7% and 0.6% respectively.The cumulative gas-generation amounts are 201.37×1011m3 and 88.39×1011m3 respectively.The average gas-generation intensities of the mudstone and coal are 250×108m3/km2 and 100×108m3/km2 respectively.The natural gas methane carbon isotopic value of Yingcheng Formation is between the cumulative carbon isotopic value of mudstone-formed methane and coal-formed methane in Xushen 1 well,which shows that hydrocarbon source rock is similar to coal measures strata of Shahezi Formation and the accumulation is a long-term in the gas pool." @default.
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- W2357251837 date "2008-01-01" @default.
- W2357251837 modified "2023-09-23" @default.
- W2357251837 title "Gas-generation evaluation of deep hydrocarbon source rocks in Xujiaweizi fault depression" @default.
- W2357251837 hasPublicationYear "2008" @default.
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