期刊文献+

三维倾斜横向各向同性介质的统一表示和模拟

General Expression and Modeling of 3D Tilted Transversely Isotropy Media in Circle Coordinate
在线阅读 下载PDF
导出
摘要 倾斜横向各向同性介质的对称轴与坐标轴有一定的旋转角度,不同的旋转方向其刚性矩阵有不同的形式.一般研究横向各向同性介质沿三个坐标轴方向旋转得到的倾斜横向各向同性介质,为了方便统一描述这类不同旋转方向的各向异性介质,提出了循环坐标系统的概念.在循环坐标系统下,容易实现各种倾斜横向各向同性介质公式的统一描述,运用到正演模拟中,可以用同一单斜介质系统的波动方程实现不同倾斜横向各向同性介质的模拟程序.最后,用三维交错网格有限差分模拟算法进行了方法的试验,结果成功地实现了三维倾斜横向各向同性介质的正演波动模拟,证实了上述概念的可行性. Tilted transversely isotropic media refer to a case of transversely isotropy with tilted symmetry axes, which have rotating angles with different stiffness matrix in different rotating directions. The cases where transversely isotropy rotates along three axes are often studied, and the concept of circle co- ordinate system is presented in order to depict them generally. In the circle ccordinate, many basic formulas of tilted transversely isotropy can be expressed easily, and a kind of monoclinic media's wave equations can be used to simulate wavefield in different tilted transversely isotropic media. The modeling algorithm is staggered grid finite difference method. The numerical steps are implemented by using second order difference in time and high-order staggered grid difference in space. Numerical results of a model show that the above concepts are reasonable and feasible, and 3D anisotropic staggered gird difference method is implemented preferably.
出处 《同济大学学报(自然科学版)》 EI CAS CSCD 北大核心 2007年第11期1556-1561,共6页 Journal of Tongji University:Natural Science
关键词 倾斜横向各向同性介质 循环坐标系统 交错网格 有限差分 正演模拟 titled transversely isotropy circle coordinate system staggered grid finite difference forward modeling
  • 相关文献

参考文献9

  • 1Thomsen L. Weak elastic anisotropy[J].Geophysics, 1986, 51 ( 10): 1954.
  • 2Ruger A. P-wave reflection coefficients for transversrly isotropic models with vertical and horizontal axis of symmetry[J]. Geohysics, 1997, 62(3) :713.
  • 3Tsvankin I. Reflection moveout and parameter estimation for horizontal transverse isotropy[J ]. Geophysics, 1997,62(2) :614.
  • 4Tsvankin I. Anisotropic parameters and P-wave velocity for orthorhombic media[J], Geophysics, 1997,62(4) : 1292.
  • 5Alkhalifah T, Tsvankin I. Velocity analysis for transversely isotropic media[J]. Geophysics, 1995,60(5) : 1550.
  • 6Hokstad K, Sqrensen L E, Maaq F. 3-D elastic finite-difference modeling in tilted transversely isotropic media [ C]//The 72^nd SEG Annual International Meeting, Expanded Abstracts. Salt Lake City:[s. n. ] ,2002:1951 - 1954.
  • 7董良国.弹性波数值模拟中的吸收边界条件[J].石油地球物理勘探,1999,34(1):45-56. 被引量:47
  • 8董良国,马在田,曹景忠,王华忠,耿建华,雷兵,许世勇.一阶弹性波方程交错网格高阶差分解法[J].地球物理学报,2000,43(3):411-419. 被引量:348
  • 9董良国,马在田,曹景忠.一阶弹性波方程交错网格高阶差分解法稳定性研究[J].地球物理学报,2000,43(6):856-864. 被引量:221

二级参考文献8

共引文献489

相关作者

内容加载中请稍等...

相关机构

内容加载中请稍等...

相关主题

内容加载中请稍等...

浏览历史

内容加载中请稍等...
;
使用帮助 返回顶部