Quick
Search: 
 
advanced search
 GSW Home    GeoRef Home    My GSW Alerts    Contact GSW    About GSW    Journals List    Help 
The Leading Edge Don't get GSW? Talk to your librarian.
JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS

The Leading Edge; July 2000; v. 19; no. 7; p. 692-701; DOI: 10.1190/1.1438692
© 2000 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 HighWire
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Koledoye, A. B.
Right arrow Articles by May, E.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

Three-dimensional visualization of normal fault segmentation and its implication for fault growth

A. Bashir Koledoye and Atilla Aydin

Stanford University, Stanford, California, U.S.

Eric May

Chevron Overseas Petroleum Incorporation, San Ramon, California, U.S.

Corresponding author: aydin@pangea.stanford.edu

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

Segmentation is a fundamental feature for all kinds of faults at different scales. It has a significant impact on hydrocarbon migration and flow for nonsealing faults, and on resevoir fluid estimates and compartmentalization for sealing faults. In spite of these benefits, application of the knowledge of fault segmentation to hydrocarbon exploration and production is limited due to poor seismic data quality, resolution, and lack of understanding of how this knowledge can be applied. Here is a case study from the Niger Delta of a normal fault seen on 3-D where we apply a methodology to visualize fault segments and their slip distribution patterns using seismic and well data.

The data set used includes a reprocessed full-fold 3-D seismic survey from offshore Niger Delta and well data from a developed oil field (Okan) in the same basin (Figures 1 and 2). The study focused on one fault system (fault X) that has excellent seismic images and numerous wireline logs from wells (Figure 2).


Figure Removed (Available Only in the Full Text)
View larger version (27K):
[in this window]
[in a new window]
 
Figure 1. Okan Field and a cross-section of the Niger Delta.

 

Figure Removed (Available Only in the Full Text)
View larger version (100K):
[in this window]
[in a new window]
 
Figure 2. Base map of Okan Field showing trace of fault X at one of the mapped time horizons. Structure contour is progressively higher from blue to green to yellow to red. Red lines are directional wells; red points are straight vertical wells. The fault dips to the southwest. Note many wells cross the fault. Stratigraphic data from wells Y and Z were used in Figure 3.

 

Figure Removed (Available Only in the Full Text)
View larger version (143K):
[in this window]
[in a new window]
 
Figure 3. (a) The major fault segments interpreted on a seismic dip line and the wells providing log data. Segments are numbered from 1 at the base to 14 at the top. Note how the relay width and segment overlap areas vary systematically from base to top. (b) Section of the line in Figure 3a (yellow box) that shows the spatial . . . [Full Text of this Article]

 



This article has been cited by other articles:


Home page
Environmental GeosciencesHome page
D. U. Ophori and D. U. Ophori
A simulation of large-scale groundwater flow in the Niger Delta, Nigeria
Environmental Geosciences, December 1, 2007; 14(4): 181 - 195.
[Abstract] [Full Text] [PDF]


Home page
AAPG BulletinHome page
A new process-based methodology for analysis of shale smear along normal faults in the Niger Delta
AAPG Bulletin, March 1, 2003; 87(3): 445 - 463.





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