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

Petroleum Geoscience; August 2005; v. 11; no. 3; p. 277-284; DOI: 10.1144/1354-079304-636
© 2005 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 Similar articles in Web of Science
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 Web of Science (1)
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Wangen, M.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

Original Article

Sandstone porosity related to vitrinite reflectance

Magnus Wangen

Institute for Energy Technology, PO Box 40 N-2027 Kjeller, Norway (e-mail: magnus@ife.no)

Vitrinite reflectance (VR) and the volume fraction of quartz cement in sandstones are both measures of thermal exposure. This paper shows how porosity reduction by quartz cementation can be related to VR for heating at a constant rate, using simple models for quartz cementation and VR. This relationship reveals that the heating rate is an explicit parameter, which means that there is no pure relationship between porosity (volume fraction quartz cement) and VR. However, the rate of quartz cementation and the rate of change of TTI (time–temperature integral) have a close exponential dependence on temperature. Porosity reduction by quartz cementation as a function of VR therefore nearly follows the same curve for very different temperature histories. This property of porosity reduction by quartz cementation is used to calibrate average specific surface parameters as a function of porosity. The calibration procedure is demonstrated on two datasets, where the average specific surface depends on porosity to the power of an exponent that is somewhat greater than 3.

KEYWORDS: vitrinite reflectance, quartz cementation, kinetics







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