Fracture properties from seismic scattering

被引：22

作者：

Massachusetts Institute of Technology, Cambridge, MA, United States ^{[1
]}

不详 ^{[2
]}

机构：

[1] Massachusetts Institute of Technology, Cambridge, MA

[2] ENI/Agip, San Donato

来源：

Leading Edge | 2007年 / 9卷 / 1186-1196期

关键词：

Acoustic wave reflection - Acoustic wave scattering - Seismic waves - Signal analysis;

D O I：

10.1190/1.2780790

中图分类号：

学科分类号：

摘要：

The seismic trace is a complex aggregate of reflected and scattered signals from subsurface formation interfaces and heterogeneities. Although many varieties of random noise may also be present in the trace, we know from reacquiring the same seismic survey that seismic data are highly repeatable, indicating that significant information about the subsurface is contained in the trace but not yet used by our standard analysis methods. Seismic scattering is a type of signal contained in the data that is generally not utilized. © 2007 Society of Exploration Geophysicists.

引用

页码：1186 / 1196

页数：10