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Regional Seismic Wavefield Computation on a 3-D Heterogeneous Earth Model by Means of Coupled Traveling Wave Synthesis

机译:基于耦合行波合成的3-D非均质地球模型区域地震波场计算

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I present a new algorithm for calculating seismic wave propagation through a three-dimensional heterogeneous medium using the framework of mode coupling theory originally developed to perform very low frequency (f <~0.01-0.05 Hz) seismic wavefield computation. It is a Greens function approach for multiple scattering within a defined volume and employs a truncated traveling wave basis set using the locked mode approximation. Interactions between incident and scattered wavefields are prescribed by mode coupling theory and account for the coupling among surface waves, body waves, and evanescent waves. The described algorithm is, in principle, applicable to global and regional wave propagation problems, but I focus on higher frequency (typically f ≥~0.25 Hz) applications at regional and local distances where the locked mode approximation is best utilized and which involve wavefields strongly shaped by propagation through a highly heterogeneous crust. Synthetic examples are shown for P-SV-wave propagation through a semi-ellipsoidal basin and SH-wave propagation through a fault zone.
机译:我提出了一种新的算法,该算法使用模式耦合理论的框架计算通过三维异质介质传播的地震波,该算法最初是为执行极低频(f <〜0.01-0.05 Hz)地震波场计算而开发的。这是一种Greens函数方法,用于在定义的体积内进行多次散射,并使用通过锁定模式近似的截断行波基集。入射波和散射波场之间的相互作用由模式耦合理论规定,并说明了表面波,体波和e逝波之间的耦合。所描述的算法原则上适用于全局和区域波传播问题,但我主要研究区域和局部距离上的较高频率(通常为f≥〜0.25 Hz)的应用,其中最好利用锁定模式近似,并且强烈涉及波场通过高度异质的地壳传播而形成。显示了通过半椭圆形盆地传播的P-SV波和通过断层带传播的SH波的合成示例。

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