首页 | 本学科首页   官方微博 | 高级检索  
     检索      

裂隙各向异性介质波场VSP多分量记录的数值模拟
引用本文:牛滨华,何樵登.裂隙各向异性介质波场VSP多分量记录的数值模拟[J].地球物理学报,1995,38(4):519-527.
作者姓名:牛滨华  何樵登
作者单位:1. 中南工业大学, 长沙 410083; 2. 长春地质学院, 长春 130026
摘    要:从各向异性介质中最为普遍的裂隙各向异性介质出发,推导了同零井源距VSP三分量观测方式相一致的一维三分量波动方程.为了更符合实际观测,引入了坐标旋转,可以模拟井中任意方位的多层各向异性介质的波场响应.用有限元方法进行了波场数值模拟,重点突出了获得凡R3×3矩阵剖面的方法,同时对R3×3,矩阵剖面进行了一般性的分析解释,事实证明,R3×3矩阵剖面含有介质丰富的各向异性信息.

关 键 词:裂隙各向异性介质  定向激发接收点  多分量观测  有限元方法  矩阵剖面  
收稿时间:1993-07-05

NUMERICAL MODELING OF VSP MULTICOMPONENT RECORDS IN CRACKS ANISOTROPIC MEDIUM
NIU BIN-HUA.NUMERICAL MODELING OF VSP MULTICOMPONENT RECORDS IN CRACKS ANISOTROPIC MEDIUM[J].Chinese Journal of Geophysics,1995,38(4):519-527.
Authors:NIU BIN-HUA
Institution:1. Central South University of Technologh, Changsha 410083; 2. Changchun Geology College, Changchun 130026
Abstract:From considering common cracks anisotropic medium in anisotropic media, 1D3-component equation is calculated. The equation is similar in zero-section VSP survey. In order to conform to readily, the paper leads into coordinate rotation so that wave field of multi-layers anisotropic media about arbitrarily azimuth in well can be modeled. Using finite element method, numerical modeling are achieved.Obtaining R3×3 matrix section is emphasized specially, and so R3×3 matrix section is ordinarily analyzed and explained. The several special wave phenomena are stressed.In fact, rich anisotropic information is contained in R3×3 matrix section.
Keywords:Cracks anisotropic media  Survey of directional shot and multicomponent recording  Finite element method  Matrix section  
本文献已被 CNKI 维普 等数据库收录!
点击此处可从《地球物理学报》浏览原始摘要信息
点击此处可从《地球物理学报》下载免费的PDF全文
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号