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; May 2005; v. 24; no. 5; p. 496-505; DOI: 10.1190/1.1926807
© 2005 Society of Exploration Geophysicists
This Article
Right arrow Figures Only
Right arrow Full Text
Right arrow Full Text (PDF)
Right arrow An erratum has been published
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 Fabricius, I. L.
Right arrow Articles by Prasad, M.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

Log interpretation of marly chalk, the Lower Cretaceous Valdemar Field, Danish North Sea

Application of iso-frame and pseudo water film concepts

Ida L. Fabricius and Casper Olsen

Technical University of Denmark, Lyngby

Manika Prasad

Colorado School of Mines, Golden, USA

Corresponding author: ilf{at}er.dtu.dk

Low-permeability marly chalk reservoirs are challenging to develop. Among the difficulties is interpretation of fluid distribution, due to the dominance of capillary forces, and a lack of cementation that might result in reservoir compaction upon draw down.






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