Lyell Collection

Geological Society, London, Special Publications

Lyell Centre  |   Lyell Collection  |   Subscriptions   |   Geological Society  |   Email alerts  |   Online bookshop  |   Help


Keywords:
Author:
Advanced search>>
This Article
Right arrow Full Text (PDF)
Right arrow References
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
Right arrow Request Permissions
Citing Articles
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Alexander, J.
Right arrow Search for Related Content
Geological Society, London, Special Publications; 1992; v. 69; p. 175-194;
DOI: 10.1144/GSL.SP.1993.069.01.08
© 1992 Geological Society of London

A discussion on the use of analogues for reservoir geology

Jan Alexander

Department of Geology, University of Wales College of Cardiff, PO Box 914, Cardiff CF1 3YE, UK

Whilst it may be easy to describe and quantify a sedimentary succession from outcrop or core, using these data to predict sedimentary facies, diagentic features and fracture distribution in unsampled areas still requires considerable intuition. Frequently, at the current state of geological knowledge, reservoir datasets must be supplemented by consideration of analogues. The aim of this paper is to sound caution on the indiscriminate use of analogues in reservoir geology.

Analogues used in reservoir geology fall into three main categories: comparisons with modern depositional processes, experimental simulations, and rock record analogues. All analogues used for reservoir geology suffer from limitations due to the physical and temporal scales at which the comparisons are made. Difficulty in selecting appropriate analogues results from the amount of interpretation of the nature of the reservoir required before an analogue may be selected, the large number of degrees of freedom in the processes of formation of reservoir rocks, and the limited numbers of well-documented analogues which are easily available.