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

Petroleum Geoscience; June 2002; v. 8; no. 2; p. 167-176
© 2002 Geological Society of London
This Article
Right arrow Figures Only
Right arrow Full Text
Right arrow Full Text (PDF)
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Right arrow Citation Map
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
Citing Articles
Right arrow Citing Articles via HighWire
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Harris, D.
Right arrow Articles by Nell, P.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

Articles

Using Shale Gouge Ratio (SGR) to model faults as transmissibility barriers in reservoirs: an example from the Strathspey Field, North Sea

D. Harris1, G. Yielding1, P. Levine3, G. Maxwell2, P. T. Rose4 and P. Nell1

1 Badleys, North Beck House, North Beck Lane, Hundleby, Spilsby PE23 5NB, UK (e-mail:david{at}badleys.co.uk)
2 Texaco North Sea Ltd, Langlands House, Aberdeen, UK (Present address: ChevronTexaco Overseas Petroleum, 4800 Fournace Place, BOB W1064, Bellaire, TX 77401-2324, USA)
3 Texaco Upstream Technology, Houston, USA (Present address: T-Surf Corporation-The GOCAD Company, 11011 Richmond Avenue, Suite 350, Houston, TX 77042, USA)
4 Texaco North Sea Ltd, Langlands House, Aberdeen, UK (Present address: Halliburton Reservoir Services, Halliburton House, Pitmedden Road, Aberdeen AB21 0GS, UK)

Since the onset of production in 1993, extraction and injection in Strathspey has focused on the central region of the field, around the ‘Central Fault’. Analysis of RFT measurements from intermittent, but regular drilling on either side of this fault has allowed reconstruction of footwall/hanging wall pore-pressure fields for particular time instances. Comparison of these similar age pressure fields shows the Central Fault capable of maintaining up to 1300 psi pressure differentials. The results of the pressure analysis were used to calibrate a fault seal attribute, termed Shale Gouge Ratio (SGR) which is an estimate of clay concentration within fault gouge, mapped across the surface of the Central Fault. The calibration showed that as SGR increases, so does the measured pressure differential across the fault. This positive relationship between SGR and pressure differential suggests SGR is a guide to potential fluid-flow resistance exerted by faults. We therefore suggest that SGR can potentially be used as a guide to defining differences in permeability within and between faults in a given field. This ‘scaleability’ of SGR as an indicator of fault permeability within a field could provide hitherto unachievable flexibility in the systematic modelling of the hydraulic behaviour of faults during fluid flow simulations.

KEYWORDS: permeability (rock), fault (geology), reservoir, fluid flow, producing




This article has been cited by other articles:


Home page
AAPG BulletinHome page
O. V. Kostenko, O. V. Kostenko, S. J. Naruk, W. Hack, M. Poupon, H.-J. Meyer, M. Mora-Glukstad, C. Anowai, and M. Mordi
Structural evaluation of column-height controls at a toe-thrust discovery, deep-water Niger Delta
AAPG Bulletin, December 1, 2008; 92(12): 1615 - 1638.
[Abstract] [Full Text] [PDF]


Home page
Petroleum GeoscienceHome page
E. A. Flodin, L. J. Durlofsky, and A. Aydin
Upscaled models of flow and transport in faulted sandstone: boundary condition effects and explicit fracture modelling
Petroleum Geoscience, April 1, 2004; 10(2): 173 - 181.
[Abstract] [Full Text] [PDF]




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