地质学
油页岩
自生的
沉积岩
陆源沉积物
矿物学
薄截面
大孔隙
白云石
地球化学
粘土矿物
水银孔隙仪
有机质
介孔材料
多孔性
化学
古生物学
岩土工程
生物化学
有机化学
多孔介质
催化作用
作者
Bixiao Xin,Xianzheng Zhao,Fang Hao,Fengming Jin,Xiugang Pu,Wenzhong Han,Qilu Xu,Pengfei Guo,Jinqiang Tian
标识
DOI:10.1016/j.coal.2022.104056
摘要
Laminae are the most typical and representive sedimentary feature in organic-rich shales, and revealing their influences on the reservoir physical properties is vital to understand the oil enrichment mechanisms of lacustrine shale. This study investigated the laminae characteristics and their effects on the physical properties of the shales from the Second Member of the Kongdian Formation (Ek 2 ). The research presented in this study is based on core and thin section observations, XRD analysis, low-pressure nitrogen physisorption (LNP), high-pressure mercury intrusion porosimetry (MIP), nuclear magnetic resonance (NMR), and scanning electron microscopy (SEM). The results show that the Ek 2 shales developed massive and laminated sedimentary structures. The laminae can be categorized as siliceous laminae, dolomite laminae, clay-rich siliceous laminae, organic matter laminae, and calcite laminae. Analysis of SEM, LNP, MIP, and NMR show that macropores and micro-fractures contribute significantly to the total pore volume of laminated samples, while micropores and mesopores are the dominant pore types in massive samples. The pore structure and connectivity of the laminated samples are better than that of the massive samples. Comparison of laminar and massive mudstones in the Ek 2 showed that the development of laminae physical properties that are more conducive for reservoir formation as a result of interlaminated fractures, optimized arrangement of minerals, and improved organic-inorganic interactions. • Five types of laminae were identified in the study area. • The development of laminae can significantly improve the reservoir physical property of shale. • The formation of interlaminated fractures may be induced by fluid overpressure, differential compaction, pressure-solution, thermal shrinkage of organic matter, or overpressure due to hydrocarcon generation.
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