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首页> 外文期刊>Pure and Applied Geophysics >Finite element analysis of fault bend influence on stick-slip instability along an intra-plate fault
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Finite element analysis of fault bend influence on stick-slip instability along an intra-plate fault

机译:断层弯曲对板内断层黏滑失稳影响的有限元分析

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摘要

Earthquakes have been recognized as resulting from stick-slip frictional instabilities along the faults between deformable rocks. A three-dimensional finite-element code for modeling the nonlinear frictional contact behaviors between deformable bodies with the node-to-point contact element strategy has been developed and applied here to investigate the fault geometry influence on the nucleation and development process of the stick-slip instability along an intra-plate fault through a typical fault bend model, which has a pre-cut fault that is artificially bent by an angle of 5.6degrees at the fault center. The numerical results demonstrate that the geometry of the fault significantly affects nucleation, termination and restart of the stick-slip instability along the intra-plate fault, and all these instability phenomena can be well simulated using the current finite-element algorithm.
机译:地震是由于沿可变形岩石之间的断层发生的粘滑摩擦不稳定性而引起的。已经开发了一种三维有限元代码,用于使用节点到点接触元素策略对可变形体之间的非线性摩擦接触行为进行建模,并将其应用于此处,以研究断层几何形状对棒形核发展过程的影响。通过典型的断层弯曲模型沿着板内断层的滑动不稳定性,该模型具有预先切割的断层,该断层在断层中心人工弯曲了5.6度角。数值结果表明,断层的几何形状显着影响板内断层的粘滑失稳的形核,终止和重新开始,并且所有这些失稳现象都可以使用当前的有限元算法很好地模拟。

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