Cookies

We use cookies to ensure that we give you the best experience on our website. You can change your cookie settings at any time. Otherwise, we'll assume you're OK to continue.


Durham Research Online
You are in:

Variation of velocity with effective stress in chalk – null result from North Sea well data.

Lubanzadio, M. and Goulty, N. R. and Swarbrick, R. E. (2002) 'Variation of velocity with effective stress in chalk – null result from North Sea well data.', Marine and petroleum geology., 19 (8). pp. 921-927.

Abstract

Wireline log data and pore pressure measurements from eight wells have been analysed to investigate how velocity in the Chalk of the Central Graben, North Sea depends on porosity and vertical effective stress. The main conclusion is that velocity shows no detectable dependence on vertical effective stress when porosity and vertical effective stress are treated as independent variables. This result contrasts with the behaviour of shales, which exhibit a reduction in velocity on unloading. The significance is that velocity in the Chalk cannot be used to detect the presence of any overpressure caused by unloading. It is suggested that the absence of an observable velocity reduction in unloaded Chalk is due to cementation.

Item Type:Article
Keywords:Over pressure, Velocity, Chalk.
Full text:Full text not available from this repository.
Publisher Web site:http://dx.doi.org/10.1016/S0264-8172(02)00135-6
Record Created:07 Jun 2010 12:20
Last Modified:08 Jun 2010 11:01

Social bookmarking: del.icio.usConnoteaBibSonomyCiteULikeFacebookTwitterExport: EndNote, Zotero | BibTex
Usage statisticsLook up in GoogleScholar | Find in a UK Library