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 Bushell, T.P.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation
Geological Society, London, Special Publications; 1986; v. 23; p. 189-208;
DOI: 10.1144/GSL.SP.1986.023.01.12
© 1986 Geological Society of London

Gas Field Studies

Reservoir Geology of the Morecambe Field

T.P. Bushell

British Gas Corporation, London, England*

The Morecambe Gas Field, located in the Irish Sea Basin, came on stream on 1 January 1985 and is to be used as a seasonal storage facility. Structurally the field is a northwest-southeast trending faulted anticline divided into two parts by a narrow southwest-northeast graben system. Gas is produced from the upper part of the Lower Triassic Sherwood Sandstone Group. The reservoir sandstones were deposited predominantly by the action of low sinuosity braided streams during periods of high stage flow. Facies associations recognised from core and wireline log data include: Channel Sandstones, Secondary and Ephemeral Channel Sandstones, Sheetflood Sandstones, Floodplain fine member and Channel abandonment deposits. Reservoir quality is dependent on grain size, shape, sorting, facies control and the distribution and abundance of authigenic cements. Quartz and dolomite cements are a major factor in causing porosity reduction, whilst authigenic illite controls effective permeability. Platy illite only occurs below an identifiable datum believed to represent a ‘paleo’ gas-water contact. Below the illite datum permeability is impaired by up to one hundred fold. A change in illite crystal morphology in the lower parts of the reservoir results in a basal zone which exhibits improved quality. The main producing horizons are stacked sandbodies within the Keuper Waterstones and Keuper Sandstone Frodsham Member. On the basis of facies modelling a three dimensional reservoir model has been developed for simulation purposes. A simplified three layer model which incorporates the influence of authigenic illite has also been erected and will control future field development. A phased development programme is planned for the field over the next ten years. The first stage is currently underway, utilising slant drilling technology to economically drain the reservoir. Maximum gas production from the field will be 1200 million cubic feet per day.


* Ultramar Exploration Ltd., 90 Long Acre, Covent Garden, London, W2CE 9RA.