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

The Leading Edge; January 2007; v. 26; no. 1; p. 66-72; DOI: 10.1190/1.2431833
© 2007 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 Whitcombe, D.
Right arrow Articles by Hodgson, L.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

Stabilizing the low frequencies

Dave Whitcombe and Linda Hodgson

BP Exploration, Aberdeen, UK

Corresponding author: david.whitcombe{at}uk.bp.com

Acoustic and elastic impedance sections have two main uses. Firstly, they "look more like geology" than traditional reflectivity data, and enable us to better communicate the subsurface images to our non-geoscientist colleagues (e.g., reservoir engineers and drillers). Secondly, inverted data can be directly calibrated to rock and fluid reservoir properties such as porosity, net-to-gross or net pay, facilitating its quantitative use.







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