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    Volume 48 Issue 6
    Jun.  2023
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    Article Navigation >  Earth Science  > 2023  >  48(6): 2267-2280
    Zhang Wei, Yang Minghui, Li Chuntang, Li Jingying, Sun Hanjing, Chong Liping, Chen Jie, Tian Gang, Xing Zhou, 2023. Structural Characteristics and Evolution of Intraplate Strike-Slip Faults in Daniudi Block, Ordos Basin. Earth Science, 48(6): 2267-2280. doi: 10.3799/dqkx.2022.477
    Citation: Zhang Wei, Yang Minghui, Li Chuntang, Li Jingying, Sun Hanjing, Chong Liping, Chen Jie, Tian Gang, Xing Zhou, 2023. Structural Characteristics and Evolution of Intraplate Strike-Slip Faults in Daniudi Block, Ordos Basin. Earth Science, 48(6): 2267-2280. doi: 10.3799/dqkx.2022.477
    shu

    Structural Characteristics and Evolution of Intraplate Strike-Slip Faults in Daniudi Block, Ordos Basin

    doi: 10.3799/dqkx.2022.477
    • 1.

      SINOPEC, North China Oil and Gas Branch Company, Zhengzhou 450006, China

    • 2.

      College of Geosciences, China University of Petroleum, Beijing 102249, China

    • 3.

      State Key Laboratory of Petroleum Resources and Prospecting, China University of Petroleum, Beijing 102249, China

    • Received Date: 2022-08-31
    • Publish Date: 2023-06-25
      Abstract
    • The intraplate strike-slip faults of the craton basin play an important role in controlling carbonate karst and reservoir formation. The faults in the main slope area of the Ordos basin are highly hidden, distributed in disorder, and difficult to analyze. At present, the research is weak, which restricts the recognition of basin tectonic evolution and multi-layer system three-dimensional reservoir formation. Guided by the structural analysis of oil area, the structural characteristics and tectonic evolution of strike-slip faults in the study area are configured and determined by using the fine interpretation of 3D seismic data of Daniudi block in Ordos basin. The study shows follows (1) there are four strike-slip faults with different strikes in Daniudi block, namely, the near NS-NNE trending Shibantai fault, the NW Tuweihe fault and the Xiaohaotu fault, and the NEE Taigemiao fault, which are characterized by vertical stratification and strike segmentation. (2) The formation and evolution of strike-slip faults in Daniudi block can be divided into four stages: Caledonian-Hercynian stage, Indosinian stage, Yanshanian stage and Himalayan stage. Among them, the right-step for left-lateral Taigemiao fault and the left-step for right-lateral northern Shibantai fault were formed from the Caledonian-Hercynian period to the Indosinian period; and the left-step for right-lateral Tuweihe fault and the right-step for left-lateral southern Shibantai fault were formed in the Yanshan period. (3)The formation background and mechanism of strike-slip faults in Daniudi block was affected by the interaction of surrounding plates. The X-type fault system composed of the northern Shibantai fault and Taigemiao fault is related to the collision and compression between the Yangtze plate and the North China craton, while the X-type fault system composed of the southern Shibantai fault and the Tuweihe fault is related to the subduction and compression of the ancient Pacific plate to the Eurasian plate.

       

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