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EARTHQUAKE ›› 2023, Vol. 43 ›› Issue (3): 18-33.doi: 10.12196/j.issn.1000-3274.2023.03.002

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3D Mesh for the Fault System in China Seismic Experimental Site

ZHANG Rong-xin1,2,3, XING Hui-lin1,2,3, SHU Tao1,2,3, LIU Jun-biao1,2,3, GUO Zhi-wei1,2,3, WANG Jian-chao1,2,3, TAN Yu-yang1,2,3   

  1. 1. Frontiers Science Center for Deep Ocean Multispheres and Earth System, Key Lab of Submarine Geosciences and Prospecting Techniques, MOE and College of Marine Geosciences, Ocean University of China, Qingdao 266100, China;
    2. Pilot National Laboratory for Marine Science and Technology (Qingdao), Qingdao 266237, China;
    3. International Center for Submarine Geosciences and Geoengineering Computing (iGeoComp), Ocean University of China, Qingdao 266100, China
  • Received:2023-03-02 Revised:2023-05-12 Online:2023-07-31 Published:2023-08-28

Abstract: The Sichuan-Yunnan region is subjected to frequent earthquakes due to the collision of the Indian and Eurasian plates, rendering it a ideal experimental site for seismic research. This paper presents a rapid method for constructing a finite element mesh model with complex faults based on a geometric mesh model of the region, using the example of the geometry model of major faults in fault system of Sichuan-Yunnan region. The following research has been conducted: ① The Advancing Front Technique (AFT) has been improved to generate a three-dimensional triangle mesh based on the geometric model, and automatically identify areas that require local refinement and conduct mesh refinement. ② An algorithm for identifying the intersection lines of intersecting faults has been proposed, and it can recognize the intersection lines between different surfaces (including fault surfaces and study area's boundaries) based on the spatial geometric relationship between non-parametric surfaces. ③ The rapid method for constructing a finite element mesh model with complex faults based on a geometric mesh model of the region has been improved. First, the original fault model is manipulated using expansion and connection operations to enable it to represent the true shape of the fault geometrically. Subsequently, the boundary of the study area and the fault mesh are combine. The intersection lines between different fault planes or between fault planes and the study area's boundary are then identified. Then, using the improved advancing front technique, the fault surface is remesh with the intersection lines as constraints to repair the mesh topology and improve the mesh quality. Finally, a tetrahedral calculation mesh model containing faults is automatically generated using the newly generated triangular mesh of the fault surface as constraints. ④ The above method has been applied to the China seismic experimental site to construct a three-dimensional calculation mesh model containing the main fault system which lays the foundation for using finite element numerical simulations to study the seismic dynamics in the study area.

Key words: Sichuan-Yunnan region, Fault system, Mesh generation, Advancing front technique

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