THE MIGRATORS EQUATION FOR ANISOTROPIC MEDIA

被引：21

作者：

UREN, NF ^{[1
]}

GARDNER, GHF ^{[1
]}

MCDONALD, JA ^{[1
]}

机构：

[1] UNIV HOUSTON,ALLIED GEOPHYS LABS,HOUSTON,TX 77204

来源：

GEOPHYSICS | 1990年 / 55卷 / 11期

关键词：

D O I：

10.1190/1.1442789

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：

The migrator's equation, which gives the relationship between real and apparent dips on a reflector in zero-offset reflection seismic sections, may be readily implemented in one step with a frequency-domain migration algorithm for homogeneous media. Huygens' principle is used to derive a similar relationship for anisotropic media where velocities are directionally dependent. Transversely isotropic media are used to demonstrate the performance of an f-k implementation of the migrator's equation for anisotropic media. Isotropic and anisotropic migration of anisotropic physical model data are compared experimentally, where the anisotropic velocity function of the medium has a vertical axis of symmetry. Only when anisotropic migration is used is the original structure recovered. -from Authors

引用

页码：1429 / 1434

页数：6

共 11 条

[1] FUNDAMENTALS OF FREQUENCY-DOMAIN MIGRATION [J].