Earth Science Frontiers ›› 2023, Vol. 30 ›› Issue (3): 181-194.DOI: 10.13745/j.esf.sf.2022.5.43

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Fluid inclusion evidence on the shale gas formation process in the Lower Cambrian Niutitang Formation in Jishou slope zone, western Hunan Province—a case study of well XJD 1

XIAO Xuewei1,2(), CHEN Honghan1,*(), LIU Xiuyan1,2, PENG Zhongqin3, LI Peijun3, WANG Baozhong3   

  1. 1. Department of Petroleum Geology, School of Earth Resources, China University of Geosciences (Wuhan), Wuhan 430074, China
    2. Key Laboratory of Tectonics and Petroleum Resources of Ministry of Education, China University of Geosciences (Wuhan), Wuhan 430074, China
    3. Wuhan Centre of Geological Survey, China Geological Survey, Wuhan 430205, China
  • Received:2022-03-02 Revised:2022-04-18 Online:2023-05-25 Published:2023-04-27

Abstract:

Southern China with frequent paleo-fluid activities possesses abundant natural resources. Based on the core data of the Lower Cambrian Niutitang Formation in Jishou slope zone, western Hunan, focusing on the black shale reservoir, we carried out a preliminary investigation of the regional fluid activities and hydrocarbon evolution through thin section, cathodoluminescence and fluid inclusion analyses and other experimental tests. The results show that dolomite, quartz and calcite minerals are deposited in the veins-both single and mixed veins-of the Niutitang Formation. Carbonate veins are mostly associated with mixed thermal fluids (upwelling fluid and seawater). The fluid inclusions are mainly bitumen, methane and saline inclusions. We identified four periods of fluid activities that are associated with hydrocarbon evolution: Early-Middle Ordovician, Early Silurian, Early-Middle Triassic and Palaeocene.

Key words: shale gas, fluid inclusion, shale gas formation process, Niutitang Formation, western Hunan Province

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