崔泽飞,朱守彪. 2023. 新生破裂影响地震破裂跨越断层阶区传播过程的扩展有限单元法模拟研究. 地震学报,45(6):1−11. doi: 10.11939/jass.20210050
引用本文: 崔泽飞,朱守彪. 2023. 新生破裂影响地震破裂跨越断层阶区传播过程的扩展有限单元法模拟研究. 地震学报,45(6):1−11. doi: 10.11939/jass.20210050
Cui Z F,Zhu S B. 2023. Extended finite element simulation study of the influence of new-cracks on the propagation of fault spontaneous ruptures across stepover. Acta Seismologica Sinica45(6):1−11. doi: 10.11939/jass.20210050
Citation: Cui Z F,Zhu S B. 2023. Extended finite element simulation study of the influence of new-cracks on the propagation of fault spontaneous ruptures across stepover. Acta Seismologica Sinica45(6):1−11. doi: 10.11939/jass.20210050

新生破裂影响地震破裂跨越断层阶区传播过程的扩展有限单元法模拟研究

Extended finite element simulation study of the influence of new-cracks on the propagation of fault spontaneous ruptures across stepover

  • 摘要: 采用扩展有限元方法计算了断层阶区内介质产生的新生破裂对地震破裂跨越断层阶区传播过程的影响。模型中新生的断层扩展遵循最大剪应力破坏准则,当最大剪应力超过岩石的承受极限时,完整介质产生破裂形成新的断层,并且新断层的扩展方向为最大剪应力方向。文中的扩展有限元法模拟结果表明,断层阶区内新生的断层改变了断层阶区的几何形态,同时也改变了断层破裂后的应力状态。新生破裂可以改变库仑应力在空间的分布格局,特别是可以提高断层上的应力水平,从而提高地震破裂跨越断层阶区的能力。模拟结果显示,由于断层阶区内新生破裂的产生,可以使得地震破裂跨越10 km宽的断层阶区,若阶区内部介质没有产生新生破裂,则地震破裂无法跨越该断层阶区。可见,本研究有助于进一步认识地震破裂跨越断层阶区的传播过程,特别是对地震震源过程分析及地震灾害评估等具有重要的科学意义。

     

    Abstract: In this paper, we employ the extended finite element method (XFEM) to assess the impact of new crack within fault stepover on the earthquake rupture propagation scenario. The initiation of new cracks in the model follows the maximum shear stress failure criterion. When the maximum shear stress surpasses the strength of rock, the intact medium undergoes fracturing, resulting in the formation of new crack. The extension direction of these new cracks aligns with the directions of maximum shear stress. Through XFEM simulation, we observe that the new crack within the fault stepover alters the fault’s geometry and the stress distribution after fault ruptures. The presence of a new crack can modify the spatial distribution pattern of Coulomb stress, particularly by increasing the stress level along the fault. Consequently, the ability of earthquake rupture propagation across a stepover is enhanced. Our simulation results demonstrate that the earthquake rupture can spread across 10-km-wide fault stepover due to the occurrence of new rupture within the stepover, and if there is no new crack in the inner part of the stepover, ruptures cannot traverse the fault stepover. Therefore, this research contributes to a deeper understanding of the earthquake spontaneous rupture propagation process across fault stepovers. The findings hold significant scientific importance for analyzing earthquake rupture propagation process and assessing earthquake disasters.

     

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