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地震波走时的有限差分法计算
引用本文:朱金明,王丽燕.地震波走时的有限差分法计算[J].地球物理学报,1992,35(1):86-92.
作者姓名:朱金明  王丽燕
作者单位:石油地球物理勘探局 河北涿州 072750
摘    要:类似于Claerbout思想,将波动方程在射线理论中的对偶--镜像方程写为上、下行波方程的形式.对变换得到的守恒型偏微分方程,用E-O格式,可计算出任意速度构造的二维网格上各点的地震波走时.文中证明了守恒型偏微分方程的通量为一凸函数,采用单调的守恒型差分格式,精度符合要求.计算速度比目前所用的各种计算走时的方法都快得多,算法也便于向量化.

关 键 词:地震波走时  有限差分  镜像方程  
收稿时间:1990-05-28

FINITE DIFFERENCE CALCULATION OF SEISMIC TRAVEL TIMES
ZHU JIN-MING WANG LI-YAN.FINITE DIFFERENCE CALCULATION OF SEISMIC TRAVEL TIMES[J].Chinese Journal of Geophysics,1992,35(1):86-92.
Authors:ZHU JIN-MING WANG LI-YAN
Institution:Bureau of Geophysical Prospecting, Hebei Zhuozhou 072750
Abstract:Similar to Claerbout' s idea, it is possible to transform the counterpart of the full wave equation in ray theory, the Eikonal equation into the form of the upgoing and/or downgoing wave equations. By application of the Engquist-Osher scheme to the transformed conservative partial differential equation, we can compute the seismic travel times of any point in a mesh with any velocity structure. The paper proves that, the flux in the conservative partial differential equation 'is a convex function. The monotone conservative finite difference scheme with first-order accuracy we used here can satisfy the accuracy demands. Its computing speed is much faster than any other travel time computing algorithms currently used. And it is vectorizable.
Keywords:Seismic travel time  Finite difference  Eikonal equation    
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