摘要
基于慢度平方三角网格剖分模型下的各向异性射线扰动理论,建立了具有垂直对称轴的横向各向同性(VTI)介质中二维QP波立体层析所需的FRECHET导数矩阵,实现了慢度平方三角网格模型的VTI介质二维QP波各向异性立体层析.考虑到各向异性参数是影响地震波运动学特征的次一级因素,制定了先反演慢度再反演各向异性参数的反演策略.由于慢度平方三角网格模型的稀疏性,使得数据空间对模型空间的FRECHET导数矩阵规模被大幅压缩,在降低了计算成本的同时也很好的保证了界面位置、背景慢度、各向异性等各个参数的反演精度.理论数据算例证实了FRECHET导数的正确性和反演策略的合理性.
Based on the anisotropic ray perturbation theory in slowness squared triangulated model,a 2D QP wave anisotropic stereo-tomography for VTI media is presented.Due to the sparsity of slowness-squared triangulated model,the scale of FRECHET derivative matrix of stereo-tomography is greatly reduced thus the computational cost is significantly cut down.Meanwhile,the accuracy of a joint inversion of the interface position,background velocity and anisotropic parameters is pretty good.The numerical examples demonstrated the correctness of the presented Frechet derivatives and the feasibility of the inversion strategy.
作者
周嘉欣
杨锴
邵炜栋
ZHOU JiaXin;YANG Kai;SHAO WeiDong(CCTEG Changzhou Research Institute,Changzhou Jiangsu 213015,China;Tiandi(Changzhou)Automation Co.,Ltd.,Changzhou Jiangsu 213015,China;State Key Laboratory of Marine Geology,Tongji University,Shanghai 200092,China;Alibaba Group,Hangzhou 311121,China)
出处
《地球物理学报》
SCIE
EI
CAS
CSCD
北大核心
2021年第11期4134-4149,共16页
Chinese Journal of Geophysics
基金
国家自然科学基金面上项目(41874118)资助.