Traveltime Calculations for qP, qSV, and qSH Waves in Two-Dimensional Tilted Transversely Isotropic Media

被引:21
作者
Huang, Guangnan [1 ,2 ]
Luo, Songting [2 ]
Deng, Juzhi [1 ]
Vavrycuk, Vaclav [3 ]
机构
[1] East China Univ Technol, Dept Geophys, Nanchang, Jiangxi, Peoples R China
[2] Iowa State Univ, Dept Math, Ames, IA 50011 USA
[3] Czech Acad Sci, Inst Geophys, Prague, Czech Republic
基金
美国国家科学基金会; 中国国家自然科学基金;
关键词
FAST SWEEPING METHOD; FINITE-DIFFERENCE CALCULATION; HAMILTON-JACOBI EQUATIONS; EIKONAL SOLVER; COMPUTATION; REFLECTION; TRANSMISSION; SCHEMES;
D O I
10.1029/2019JB018868
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
This paper presents a fast sweeping method (FSM) to calculate the first-arrival traveltimes of the qP, qSV, and qSH waves in two-dimensional (2D) transversely isotropic media, whose symmetry axis may have an arbitrary orientation (tilted transverse isotropy [TTI]). The method discretizes the anisotropic eikonal equation with finite difference approximations on a rectangular mesh and solves the discretized system iteratively with the Gauss-Seidel iterations along alternating sweeping orderings. At each mesh point, a highly nonlinear equation is solved to update the numerical solution until its convergence. For solving the nonlinear equation, an interval that contains the solutions is first determined and partitioned into few subintervals such that each subinterval contains one solution; then, the false position method is applied on these subintervals to compute the solutions; after that, among all possible solutions for the discretized equation, a causality condition is imposed, and the minimum solution satisfying the causality condition is chosen to update the solution. For problems with a point-source condition, the FSM is extended for solving the anisotropic eikonal equation after a factorization technique is applied to resolve the source singularities, which yields clean first-order accuracy. When dealing with the triplication of the qSV wave, solutions corresponding to the minimal group velocity are chosen such that continuous solutions are computed. The accuracy, efficiency, and capability of the proposed method are demonstrated with numerical experiments.
引用
收藏
页数:20
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