On the computation of the Frechet derivatives for seismic waveform inversion in 3D general anisotropic, heterogeneous media

被引:14
作者
Zhou, Bing [1 ]
Greenhalgh, Stewart [1 ,2 ]
机构
[1] Univ Adelaide, Dept Phys, Adelaide, SA, Australia
[2] Swiss Fed Inst Technol, Inst Geophys, Zurich, Switzerland
关键词
FREQUENCY TRAVEL-TIMES; ELASTIC INVERSION; ADJOINT METHODS; BODY WAVES; PART; SENSITIVITY; TOMOGRAPHY; KERNELS; FIELD; STRATEGY;
D O I
10.1190/1.3123766
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
We present a perturbation method and amatrix method for formulating the explicit Frechet derivatives for seismic body-wave waveform inversion in 3D general anisotropic, heterogeneous media. Theoretically, the two methods yield the same explicit formula valid for any class of anisotropy and are completely equivalent if the model parameterization in the inversion is the same as that used in the discretization scheme (unstructured or structured mesh) for forward modeling. Explicit formulas allow various model parameterization schemes that try to match the resolution capability of the data and possibly reduce the dimensions of the Jacobian matrix. Based on the general expressions, relevant formulas for isotropic and 2.5D and 3D tilted transversely isotropic (TTI) media are derived. Two computational schemes, constant-point and constant- block parameterization, offer effective and efficient means of forming the Jacobian matrix from the explicit Frechet derivatives. The sensitivity patterns of the displacement vector to the independent model parameters in a weakly anisotropic medium clearly convey the imaging capability possible with seismic waveform inversion in such an anisotropic medium.
引用
收藏
页码:WB153 / WB163
页数:11
相关论文
共 47 条