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    Volume 44 Issue 3
    Mar.  2019
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    Article Navigation >  Earth Science  > 2019  >  44(3): 953-971
    Wang Ye, Qiu Nansheng, Yang Yunfeng, Rui Xiaoqing, Zhou Yuanyuan, Fang Guangjian, Wu Hang, Shen Baojian, Cheng Lijun, 2019. Thermal Maturity of Wufeng-Longmaxi Shale in Sichuan Basin. Earth Science, 44(3): 953-971. doi: 10.3799/dqkx.2018.125
    Citation: Wang Ye, Qiu Nansheng, Yang Yunfeng, Rui Xiaoqing, Zhou Yuanyuan, Fang Guangjian, Wu Hang, Shen Baojian, Cheng Lijun, 2019. Thermal Maturity of Wufeng-Longmaxi Shale in Sichuan Basin. Earth Science, 44(3): 953-971. doi: 10.3799/dqkx.2018.125
    shu

    Thermal Maturity of Wufeng-Longmaxi Shale in Sichuan Basin

    doi: 10.3799/dqkx.2018.125
    • 1.

      State Key Laboratory of Petroleum Resources and Prospecting, China University of Petroleum, Beijing 102249, China

    • 2.

      College of Geosciences, China University of Petroleum, Beijing 102249, China

    • 3.

      Wuxi Research Institute of Petroleum Geology, SINOPEC Petroleum Exploration and Production Research Institute, Wuxi 214126, China

    • 4.

      State Key Laboratory of Shale Oil and Gas Enrichment Mechanisms and Effective Development, Wuxi 214126, China

    • 5.

      Chongqing Engineering Research Center for Shale Gas Resource & Exploration, Chongqing Institute of Geology and Mineral Resources, Chongqing 400042, China

    • Received Date: 2018-09-14
    • Publish Date: 2019-03-15
      Abstract
    • The marine shale of Upper Ordovician Wufeng Formation (O3w)-Lower Silurian Longmaxi Formation (S1l) is the main source rock and the target of shale gas exploration in Sichuan Basin.Organic matter maturity is not only the key to evaluate hydrocarbon generation, but also a vital indicator of shale quality evaluation.The maturity of organic matter in Lower Paleozoic shale has always been a difficult and hot issue in organic petrology.However, the previous studies were focused on the conversion of solid bitumen reflectance to equivalent vitrinite reflectance on account of the lack of vitrinite in Lower Paleozoic stratum.And the limitation and uncertainty of bitumen give rise to a lack of uniform understanding and systematic research of Wufeng-Longmaxi shale on thermal maturity.The core and outcrop samples of Wufeng-Longmaxi shale were collected in Sichuan Basin and its periphery areas for optical analysis of organic matter.The macerals and optical characteristics of various organic matter in Wufeng-Longmaxi shale were analyzed.The main macerals organic components are composed of the graptolite fragments and solid bitumen.Two types of solid bitumen have been distinguished in shales, based on optical properties and microstructure characteristics in reflected light:(1) pyrobitumen—a highly reflecting granular and sharp angular bitumen accumulates in intergranular pore spaces and microfractures; (2) matrix solid bitumen—an irregular granular surface and finely organic matter particle widely disseminated in the clay mineral matrix with low reflectance.The random reflectance of pyrobitumen is slightly lower than that of graptolite in the same sample.The increase of graptolite reflectance is faster than that of solid bitumen with the increase of maturity, and anisotropy increases significantly.Both pyrobitumen and graptolite can be used for maturity analysis in Lower Paleozoic shale.Compared to the reflectance of solid bitumen, the random reflectance of graptolite is more suitable as maturity index due to reflectance value show a narrower range.However, its relationship with vitrinite reflectance at overmature stage still needs further study.

       

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