盆地多尺度构造驱动的流体-岩石作用及成储效应

李忠; 罗威; 曾冰艳; 刘嘉庆; 于靖波

doi:10.3799/dqkx.2018.323

Volume 43 Issue 10

Oct. 2018

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Article Navigation > Earth Science > 2018 > 43(10): 3498-3510

Li Zhong, Luo Wei, Zeng Bingyan, Liu Jiaqing, Yu Jingbo, 2018. Fluid-Rock Interactions and Reservoir Formation Driven by Multiscale Structural Deformation in Basin Evolution. Earth Science, 43(10): 3498-3510. doi: 10.3799/dqkx.2018.323

Citation:

Li Zhong, Luo Wei, Zeng Bingyan, Liu Jiaqing, Yu Jingbo, 2018. Fluid-Rock Interactions and Reservoir Formation Driven by Multiscale Structural Deformation in Basin Evolution. Earth Science, 43(10): 3498-3510. doi: 10.3799/dqkx.2018.323

Citation:

Li Zhong, Luo Wei, Zeng Bingyan, Liu Jiaqing, Yu Jingbo, 2018. Fluid-Rock Interactions and Reservoir Formation Driven by Multiscale Structural Deformation in Basin Evolution. Earth Science, 43(10): 3498-3510. doi: 10.3799/dqkx.2018.323

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Fluid-Rock Interactions and Reservoir Formation Driven by Multiscale Structural Deformation in Basin Evolution

doi: 10.3799/dqkx.2018.323

1.
Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China
2.
University of Chinese Academy of Sciences, Beijing 100049, China

Received Date: 2018-05-11
Publish Date: 2018-10-20

Abstract

Abstract

Fluid-rock interactions in sedimentary basins have been focused on the non-structural genetic mechanisms on medium and small scales in most papers published, which has constrained the understanding of the objective laws on basin-scale. The conceptual models or working modes of fluid-rock interactions driven by structural deformation (FRIDSD) in sedimentary basin evolution are presented in this paper. Conbined with the typical cases on carbonate and clastic reservoirs studied, key processes, control factors and reservoir-forming effects of FRIDSD are analysed and discussed. It is indicated that there are significant differences of FRIDSD between carbonates and sandstones in the type, intensity and distribution, exist between carbonates and sandstones. For carbonate reservoirs, it cannot be neglected that, even in weak structural deformation, dissolution and filling-cementation of carbonates related to a lot of microcracks also develop over structural traps. On the other hand, for clastic (sandstone) reservoirs, diagnostic deformation bands and their related structural diagenesis, with few microcracks, develop in weak structural deformation. However, intensive structural deformation most probably makes more (micro-) cracks and promotes FRIDSD in sandstones, which may also improve the deep-buried reservoir property to a certain extent. It is pointed out that key problems of FRIDSD mainly include intensive change of fluid pressure, petrological-mineral stabilities modified by strain, intensive/rapid change of reactive surface and volume on fluid-rock interactions.
- structural deformation,
- fluid-rock interaction,
- carbonate reservoir,
- clastic reservoir,
- basin geodynamics,
- petroleum geology

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References(74)

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