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    Volume 43 Issue 7
    Jul.  2018
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    Wang Baozhong, Ou Wenjia, Wang Chuanshang, Peng Zhongqin, Zhang Guotao, 2018. Geochemical Characteristics of the Early Carboniferous Shale in Guizhong Depression and Their Contribution to Adjacent Gas Reservoirs. Earth Science, 43(7): 2222-2233. doi: 10.3799/dqkx.2018.226
    Citation: Wang Baozhong, Ou Wenjia, Wang Chuanshang, Peng Zhongqin, Zhang Guotao, 2018. Geochemical Characteristics of the Early Carboniferous Shale in Guizhong Depression and Their Contribution to Adjacent Gas Reservoirs. Earth Science, 43(7): 2222-2233. doi: 10.3799/dqkx.2018.226

    Geochemical Characteristics of the Early Carboniferous Shale in Guizhong Depression and Their Contribution to Adjacent Gas Reservoirs

    doi: 10.3799/dqkx.2018.226
    • Received Date: 2017-08-20
    • Publish Date: 2018-07-15
    • To date there are only a few studies on genetic potential of the Early Carboniferous shale in Guizhong depression, which severely restricts the unconventional oil and gas exploration (mainly shale gas) in this area. In this study, typical profile measurements and sampling analysis of the shale from the Early Carboniferous slope facies in Guizhong depression were conducted, and then the hydrocarbon generating potential of the shale was discussed from multiple perspectives, including the TOC content, rock pyrolysis, organic carbon isotope composition, n-alkane composition and the vitrinite reflectance of the shale. Combined with regional tectonic evolution history, three models of near source gas reservoirs, which are closely related to the shale from the Lower Carboniferous Yanguanian Stage, are summarized. The results show that, TOC values are ranging from 0.25% to 15.67%. The shales deposited before forced regressive are rich in organic matter, with TOC values greater than 2%. There are weak positive correlations between TOC value and chloroform bitumen "A", the hydrocarbon generating potential and the total hydrocarbon respectively. The type of the organic metter in the shales is mainly classified as kerogen type Ⅱ. The values of Ro are ranging from 1.72% to 2.78%, in the overmature stage. According to the lithologic characteristics and the present tectonic position of Guizhong depression, we suggest that the ramp structure zone in the middle of the depression is favorable for the formation of near source gas reservoirs, while the back thrust zone is poor. The thrust nappe structure zone in the edge of the depression is the near source gas accumulation zone with lithologic traps.

       

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