快速推进法在地震波传播正演模拟中的应用

W. Srigutomo, Ghany Hanifan Muslim
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引用次数: 1

摘要

在给定的非均质介质中,确定地震波在两点之间的时间传播和射线路径是地震学中的经典问题之一。这个问题用eikonal方程表示,可以看作是波前和界面演化的传播。解决这一问题的方法之一是快速推进法,简称FMM。用该方法求出了满足熵的eikonal方程粘度解。FMM结合Hamilton-Jacobi方程的黏度解和以最小堆数据结构为中心的Huygen原理,确定每循环处的最小值。在本研究中,FMM被用于确定地震波的时间旅行和射线路径。用简单的算法,利用FMM确定了波源的位置。从我们的正演模拟方案中发现,FMM是一种准确、鲁棒和有效的模拟地震波传播的方法。为了进一步研究,FMM也可以作为被动地震反演方案的一部分来定位震源位置。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Fast Marching Method Aplication for Forward Modelling of Seismic Wave Propagation
One of the classical problem in seismology is to determine time travel and ray path of seismic wave betweentwo points at a given heterogeneous media. This problem is expressed by eikonal equation and can be seen as a propagation of a wavefront and interface evolution. One of methods to solve this problem is Fast Marching Method abbreviated as FMM. This method is used to produce entropy-satisfying viscosity solution of eikonal equation. FMM combines viscosity solution of Hamilton-Jacobi equation and Huygen's Principle that centered on min-heap data structure to determine the minimum value at every loop. In this study, FMM is applied to determine time travel and raypath of seismic wave. FMM also is used to determine the location of wavesource using simple algorithm. From our forward modeling schemes, it is found that FMM is an accurate, robust, and effcient method to simulate seismic wave propagation. For further study, FMM also can be used to be a part of passive seismic inverse scheme to locate hypocenter location.
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