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层状横向各向同性介质反问题初探
引用本文:宋海斌,张关泉.层状横向各向同性介质反问题初探[J].地球物理学报,1997,40(1):105-119.
作者姓名:宋海斌  张关泉
作者单位:1. 同济大学海洋地质与地球物理系, 上海 200092; 2. 中国科学院计算数学和科学工程计算研究所, 北京 100080
基金项目:国家自然科学基金,中国科学院资助,中国石油天然气总公司和大庆石油管理局资助
摘    要:用偏微分方程组特征理论研究层状并以垂直轴为对称轴的横向各向同性(TIV)介质的参数反演问题,首先从弹性波运动方程与TIV介质的应力-应变关系导出了平面波耦合方程组的特征型.根据奇性分析与特征积分法给出了连续情形下的特征线边界条件,连续清形下的波场延拓方程即平面波耦合方程组的特征型与特征线边界条件组成了层状TIV平滑介质、弱间断介质参数反演问题的基本方程组.并导出了间断情形下的波场延拓方程与特征线边界条件,这些方程组可用于层状介质(间断情况)的参数反演.基于这些基本方程组,探讨了利用地面多分量地震资料反演层状TIV介质多个弹性参数的问题.

关 键 词:特征理论  弹性波反演  层状介质  横向各向同性介质  
收稿时间:1995-07-10

A PRIMARY STUDY ON AN INVERSE PROBLEM FOR STRATIFIED TRANSVERSELY ISOTROPIC MEDIA
SONG HAI-BIN, MA ZAI-TIAN.A PRIMARY STUDY ON AN INVERSE PROBLEM FOR STRATIFIED TRANSVERSELY ISOTROPIC MEDIA[J].Chinese Journal of Geophysics,1997,40(1):105-119.
Authors:SONG HAI-BIN  MA ZAI-TIAN
Institution:1. Tongji University, Shanghai 200092, China; 2. Institute of Computational Mathematics and Scientific / Engineering Computing, Academia Sinica, Beijing 100080, China
Abstract:A study is conducted of inversion of elastic parameters in stratified transverselyisotropic media with a vertical axis of symmetry (TIV media) by using partial differentialsystem characteristic theory. At first, the characteristic type of plane wave coupledequations are derived from equation of motion and stress-strain relation. Thencharacteristic line boundary condition expressions (continued situation) are given throughmethods of singularity analysis and characteristic line integral. These two systems arebasic equations for inversion of elastic parameters in stratified smooth media or weaklydiscontinued TIV media, Besides, wavefield extrapolation formulae and characteristicline boundary condition expressions corresponding to discontinued situation are also attained and can be used for inversion of elastic parameters in stratified TIV media(discontinued situation). At last, it is considered how to reconstruct simultaneouslyseveral or six elastic parameters (density and five dependent stiffness coefficients)from multi-wave multi-component seismic data at the surface through analysis ofthese basic systems.
Keywords:Characteristic theory  Elastic wave inversion  Stratified media  Transverse isotropy
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