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Boundary integral equations for dynamic rupture propagation on vertical complex fault system in half-space: Theory

机译:半空间垂直复杂断层系统中动态破裂扩展的边界积分方程:理论

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Abstract The boundary integral equation method (BIEM) is now widely used in numerical studies on earthquake rupture dynamics, and is proved to be a powerful tool to deal with problems on complex fault system. However, since this method heavily lies on the specific forms of Green’s function and only the Green’s function in full-space has a closed analytic expression, it is usually limited to a full-space medium. In this study, as a first step to extend this method to an arbitrary complex fault system in half-space, the boundary integral equations (BIEs) for dynamic strike-slip on vertical complex fault system in half-space are derived based on exact Green’s function for isotropic and homogeneous half-space. Effect of the geometry of the complex fault system are dealt with carefully. Final BIEs is composed of two parts: contribution from full-space, which has been thoroughly investigated by Aochi and his co-workers by using the Green’s function for full-space, and that from free surface, which is studied in detail in this study.
机译:摘要边界积分方程法(BIEM)在地震破裂动力学数值研究中得到了广泛的应用,被证明是解决复杂断层系统问题的有力工具。但是,由于此方法在很大程度上取决于Green函数的特定形式,并且只有全空间的Green函数具有封闭的解析表达式,因此通常仅限于全空间介质。在这项研究中,作为将此方法扩展到半空间中任意复杂断层系统的第一步,基于精确格林定律,推导了半空间中垂直复杂断层系统上动态走滑的边界积分方程(BIE)。各向同性和均质半空间的功能。复杂故障系统的几何形状影响要仔细处理。最终的BIE由两部分组成:Aochi和他的同事们通过使用Green的全空间功能对全空间的贡献进行了彻底的研究,而自由表面则对此进行了详细研究。 。

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