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    Volume 44 Issue 3
    Mar.  2019
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    Wu Xiaoqi, Chen Yingbin, Liu Quanyou, Wang Ping, Zeng Huasheng, Wang Yanqing, Hu Ye, Li Huaji, 2019. Molecular Geochemical Characteristics of Source Rocks in the 5th Member of Upper Triassic Xujiahe Formation, Xinchang Gas Field, West Sichuan Depression. Earth Science, 44(3): 859-871. doi: 10.3799/dqkx.2018.236
    Citation: Wu Xiaoqi, Chen Yingbin, Liu Quanyou, Wang Ping, Zeng Huasheng, Wang Yanqing, Hu Ye, Li Huaji, 2019. Molecular Geochemical Characteristics of Source Rocks in the 5th Member of Upper Triassic Xujiahe Formation, Xinchang Gas Field, West Sichuan Depression. Earth Science, 44(3): 859-871. doi: 10.3799/dqkx.2018.236

    Molecular Geochemical Characteristics of Source Rocks in the 5th Member of Upper Triassic Xujiahe Formation, Xinchang Gas Field, West Sichuan Depression

    doi: 10.3799/dqkx.2018.236
    • Received Date: 2018-10-09
    • Publish Date: 2019-03-15
    • The 5th member of the Upper Triassic Xujiahe Formation (T3x5) is one of the important targets for terrigenous natural gas exploration in the Xinchang gas field in the West Sichuan Depression.The molecular geochemical characteristics have been analyzed in order to further determine the sedimentary environment of the T3x source rocks.The studies indicate that the Pr/Ph ratio of soluble extract from the T3x5 mudstone in the Xinchang gas field ranges from 0.26 to 1.70, and the relative contents of C27 and C29 in C27-C29 regular steranes are 31.2% and 44.6%, respectively.The gammacerane/C30 hopane ratio ranges from 0.11 to 0.34, and the MPI1, F1 and 4-/1-MDBT values of the T3x5 mudstone are all positively correlated with thermal maturity.The organic source of the T3x5 mudstone is dominated by terrigenous higher plant, and lower hydrobiont and algae have also made a certain contribution.The T3x5 mudstone was mainly deposited in the lacustrine environment, with part of the samples in the anoxic saline environment.Thermal maturity can significantly affect several indexes of aromatic compounds in coal-measure source rocks, and the three fluorene series of samples with Ro>1.25% and MDBTs/MDBFs ratios of samples with Ro>1.2% can not be directly used to determine the sedimentary environment.

       

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