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    Volume 48 Issue 4
    Apr.  2023
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    Qu Mengxue, Cheng Xiaogan, Tian Hefeng, Chen Hanlin, Yu Hongzhou, Chen Changjin, Sun Siyao, 2023. Effect of Double-Décollement Strength on Structure Deformation in Northern Bogda Mountain Using Discrete Element Numerical Simulation. Earth Science, 48(4): 1366-1378. doi: 10.3799/dqkx.2022.228
    Citation: Qu Mengxue, Cheng Xiaogan, Tian Hefeng, Chen Hanlin, Yu Hongzhou, Chen Changjin, Sun Siyao, 2023. Effect of Double-Décollement Strength on Structure Deformation in Northern Bogda Mountain Using Discrete Element Numerical Simulation. Earth Science, 48(4): 1366-1378. doi: 10.3799/dqkx.2022.228

    Effect of Double-Décollement Strength on Structure Deformation in Northern Bogda Mountain Using Discrete Element Numerical Simulation

    doi: 10.3799/dqkx.2022.228
    • Received Date: 2022-04-08
    • Publish Date: 2023-04-25
    • The fold-thrust belt of the northern Bogda Mountain is characterized by horizontal segmentation, vertical stratification, overlap of multi-phase structure deformation and rich pre-existing structures. Two décollements, the Xishangyao Formation of Upper Jurassic and the Badaowan Formation of Lower Jurassic, are developed in this area. In order to investigate the influence of the difference in cohesion strength between the two décollements and the pre-existing structures on the structure deformation in Cenozoic, this study designed five experiments including a model without décollement and four double-décollement models with different cohesion strength combinations adopted the discrete element method, on the basis of laying out pre-existing structures. The experimental results show that when the cohesion strengths of the double-décollement are the same, the upper décollement has the advantage in stress propagation; when the cohesion strengths of the double-décollement are different, the stress will preferentially transmits along the weaker cohesion décollement, and when the cohesion strength of the lower décollement is weaker, the upper décollement may not play a role. By comparing the experimental results with actual geological profile, it is concluded that the pre-existing structures control the structure deformation style of the thrust belt. However, the two décollements jointly control the tectonic decoupling in the vertical of the fold-thrust belt, and that the cohesion strength of the upper décollement weaker than that of the lower décollement, which is a key factor affecting the Cenozoic structure deformation in the study area.

       

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