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    中国百强科技报刊

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    Volume 48 Issue 2
    Feb.  2023
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    Article Contents
    Liu Zhaoqian, Ma Liyuan, He Xinyue, Wen Lifeng, Tang Yong, Zheng Rongchen, Re Yuting, Luo Xing, 2023. Tectonic Deformation Sequence, Critical Tectonic Periods and Characteristics in Dongsheng Gas Field, Ordos Basin, China. Earth Science, 48(2): 533-552. doi: 10.3799/dqkx.2022.416
    Citation: Liu Zhaoqian, Ma Liyuan, He Xinyue, Wen Lifeng, Tang Yong, Zheng Rongchen, Re Yuting, Luo Xing, 2023. Tectonic Deformation Sequence, Critical Tectonic Periods and Characteristics in Dongsheng Gas Field, Ordos Basin, China. Earth Science, 48(2): 533-552. doi: 10.3799/dqkx.2022.416

    Tectonic Deformation Sequence, Critical Tectonic Periods and Characteristics in Dongsheng Gas Field, Ordos Basin, China

    doi: 10.3799/dqkx.2022.416
    • Received Date: 2022-11-29
    • Publish Date: 2023-02-25
    • The nor-marine tight sandstone strata of upper Paleozoic contains rich hydrocarbon resources in Dongsheng gas field in Hangjinqi area, northern Ordos Basin. But the western, eastern, and northern margin mountains surround northern Ordos Basin which experienced multiphase, multi-direction and multi-attribute tectonization. The nor-marine tight sandstone strata of upper Paleozoic in Hangjinqi area exhibit large differences of structural effect, tight and strong heterogeneous reservoirs, complicated and specific hydrocarbon geological characteristics. Based on relationship analysis between northern basin and surrounding margin tectonic systems, stratigraphic contact relationship, 3D-seismic data, paleogeomorphic and tectonic chronology analysis, three main fault systems properties and formation time have been identified. (1)EW-NEE-trend faults are compressional fault at Late Jurassic and tensional fault at Late Cretaceous-early Himalayan epoch. (2)NW-NWW-trend faults are tensional strike slip fault at Late Cretaceous-early Himalayan epoch. (3)NE-SN-trend faults are compressional fault tensional fault at Early Cretaceous and tensional strike slip fault at Late Cretaceous-early Himalayan epoch. Three periods of tectonic deformation have been identified, which are Late Jurassic, Early Cretaceous and Late Cretaceous-early Himalayan epoch. Two critical tectonic periods have been identified which are the Early Yanshan epoch (late Jurassic-early Cretaceous) and the Later Yanshan epoch-early Himalayan epoch (later Cretaceous-early Eocene). The control effect of two critical tectonic periods on nor-marine tight gas accumulation express as different pattern, spatial extent, and results.

       

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