Xinjiang Petroleum Geology ›› 2025, Vol. 46 ›› Issue (5): 521-530.doi: 10.7657/XJPG20250501

• OIL AND GAS EXPLORATION •     Next Articles

Characteristics and Controlling Factors of Pore Structure in Coal-Measure Shale Reservoirs: Taking Longtan Formation in Western Guizhou as an Example

LI Juhao1(), HE Jinxian1(), YANG Zhaobiao1, ZHANG Xiaoli1, WU Meng2, MA Li3, YUAN Yuan4,5, WEN Mingzhong2   

  1. 1. China University of Mining and Technology, a.MOE Key Laboratory of Coalbed Methane Resources & Reservoir Formation Process; b.School of Resources and Geosciences, Xuzhou, Jiangsu 221116, China
    2. Jiangsu Design Institute of Geology and Mineral Resources / Testing Center of China National Administration of Coal Geology, Xuzhou, Jiangsu 221006, China
    3. Shanxi Branch of China National Geological Exploration Center of Building Materials Industry, Taiyuan, Shanxi 030031, China
    4. Shanxi Coal Geology No.115 Exploration Institute Co., Ltd., Datong, Shanxi 037000, China
    5. Shanxi Technology Innovation Center for Comprehensive Monitoring & Emergency Disaster Mitigation in Mines, Datong, Shanxi 037000, China
  • Received:2024-12-20 Revised:2025-02-03 Online:2025-10-01 Published:2025-09-30

Abstract:

Pore structure affects gas storage performance of shale and is an important parameter for evaluating shale gas resource potential. Taking the coal-measure shale of Upper Permian Longtan formation in western Guizhou as an example, micro-pores and micro-fractures were qualitatively observed using scanning electron microscopy (SEM) and classified, and the microscopic pore structure and pore size distribution were quantitatively characterized through high-pressure mercury injection and low-temperature nitrogen adsorption experiments. Combining with organic geochemical parameters and mineral composition distribution characteristics, the factors controlling the pore structures of coal-measure shale reservoirs were identified. The results show that the matrix pores in coal-measure shale of the Longtan formation can be divided into six occurrence types: residual primary intergranular pores, mineral moldic pores, clay mineral intergranular pores, intergranular pores, intragranular dissolution pores, and organic pores, and the micro-fractures are mainly extensional, shear, bedding, and diagenetic shrinkage micro-fractures. Micro-pores (especially those with diameter <5 nm) and transitional pores provide the main pore space. The pore space types are dominated by ink bottle holes and V-shaped holes, with a certain amount of parallel slits, and the connectivity between pores is relatively good. Total organic carbon content (TOC), maturity of organic matter, and mineral composition are the main factors controlling the pore structure of the coal-measure shale reservoirs of Longtan formation in western Guizhou. The single-point pore volume and specific surface area of the shale increase with the increase of TOC. The degree of thermal evolution contributes positively to the increase of micro-pore and transitional pore volume. Clay minerals have complex impacts on the pore structure. High brittleness index has a positive effect on the development of meso-pores, macro-pores and micro-fractures, being conducive to shale gas flow.

Key words: western Guizhou, Longtan formation, coal-measure shale, shale gas, pore structure, controlling factor

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