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    Volume 48 Issue 12
    Dec.  2023
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    Article Navigation >  Earth Science  > 2023  >  48(12): 4540-4557
    Yan Zhaokun, Li Yong, Nie Zhou, Ren Cong, Shao Chongjian, Dong Shunli, Zhang Daizhu, Ye Tingting, 2023. Evolution Process and Dynamic Mechanism of Luzhou-Kaijiang Paleo-Uplift during Indosinian, China. Earth Science, 48(12): 4540-4557. doi: 10.3799/dqkx.2022.085
    Citation: Yan Zhaokun, Li Yong, Nie Zhou, Ren Cong, Shao Chongjian, Dong Shunli, Zhang Daizhu, Ye Tingting, 2023. Evolution Process and Dynamic Mechanism of Luzhou-Kaijiang Paleo-Uplift during Indosinian, China. Earth Science, 48(12): 4540-4557. doi: 10.3799/dqkx.2022.085
    shu

    Evolution Process and Dynamic Mechanism of Luzhou-Kaijiang Paleo-Uplift during Indosinian, China

    doi: 10.3799/dqkx.2022.085
    • 1.

      State Key Laboratory of Nuclear Resources and Environment, East China University of Technology, Nanchang 330013, China

    • 2.

      Key Laboratory of Deep-Earth Dynamics, Ministry of Natural Resources, Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China

    • 3.

      State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Chengdu University of Technology, Chengdu 610059, China

    • 4.

      Southwest Oil & Gas Field Company, PetroChina, Chengdu 610041, China

    • Received Date: 2021-08-20
      Available Online: 2024-01-03
    • Publish Date: 2023-12-25
      Abstract
    • The Indosinian Luzhou-Kaijiang paleo-uplift is located in the eastern part of Sichuan basin. It has been paid more attention due to the petroleum geological significance of the karst unconformity on the paleo-uplift. However, there is a debate to the evolution process and dynamic mechanism of Luzhou-Kaijiang paleo-uplift, which has affected both the understanding on the Indosinian tectonic evolution of Upper Yangtze block and the exploration of oil and gas in Sichuan basin. The unconformity on the Luzhou-Kaijiang paleo-uplift will be analyzed in detail, based on the seismic, drilling and field outcrop data. Combined with regional tectonic events and global sea level change, the evolution process and dynamic mechanism of the paleo-uplift will be studied systematically using the evolution model of foreland basin system. It is considered that the Luzhou-Kaijiang paleo-uplift was formed and developed in the Late Triassic Carnian to Norian, and died in the Rhaetian. The Luzhou-Kaijiang paleo-uplift is a component unit (forebulge) of the Late Triassic Longmenshan foreland basin system. Its formation was driven by the tectonic load of the Longmenshan orogenic wedge and the sedimentary load in the foreland basin. The evolution process of the paleo-uplift was mainly controlled by the thrust and nappe of the Longmenshan orogenic wedge toward the Yangtze block, which was probably resulted from southeastward shortening of the western margin of the Yangtze block in response to the Late Triassic convergence among Qiangtang, Yangtze and North China blocks.

       

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