Quick
Search: 
 
advanced search
 GSW Home    GeoRef Home    My GSW Alerts    Contact GSW    About GSW    Journals List    Help 
The Leading Edge Signup for GSW Email News
JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS

The Leading Edge; March 2004; v. 23; no. 3; p. 232-239; DOI: 10.1190/1.1690895
© 2004 Society of Exploration Geophysicists
This Article
Right arrow Figures Only
Right arrow Full Text
Right arrow Full Text (PDF)
Right arrow Submit a response
Right arrow Alert me when this article is cited
Right arrow Alert me when eLetters are posted
Right arrow Alert me if a correction is posted
Services
Right arrow Email this article to a friend
Right arrow Similar articles in this journal
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Right arrow reprints & permissions
Citing Articles
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Fairborn, J.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

Unstacked migrated traces for AVO and velocity analysis

John Fairborn

WellSeismic Computing Services, Newport Beach, California, U.S.

Corresponding author: johnf@wellseismic.com

The first 20% of the full text of this article appears below.

There are a number of reasons why it would be nice to directly map reflections on a time trace to their image point in depth without all the trace mixing required by conventional migration. Such one-to-one mapping would preserve the shot and receiver coordinates of the trace, thereby allowing reflections to be modeled within the framework of the data.

Consider what must be done now for velocity analysis using reflection tomography or for AVO analysis on depth-migrated traces. The first step is to create common image gathers of traces over a range of offsets. This necessitates a series of common-offset migrations at selected image points (defined here as an x-y location on the migrated image) in which a large number of traces are mixed together and, consequently, the concept of a shot-receiver location for each migrated trace is lost. If there is structural dip or a lateral velocity gradient, this loss of trace geometry poses a problem for both AVO and reflection tomography because the next step is ray tracing. We have a reflection point and an offset, but to proceed with the ray tracing either the dip or a shot-receiver coordinate is required. Because the shot-receiver coordinate is lost in the migration process, the dip must be known. This is what is meant by going outside the framework of the data—a model of reflecting surfaces must be constructed by looking at preliminary migrations, and then the rays must be traced by some trial and error procedure until the incident and reflection angles are as they should be for a given offset.

The process can be made somewhat efficient, but still it takes time, can be tedious, and is subject to error if the modeled surfaces are seriously in error. For tomography, where iterations are often required, this procedure may . . . [Full Text of this Article]







JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS
Copyright © 2009 by Society of Exploration Geophysicists