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
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 Hatton, I. R.
Right arrow Articles by Roberts, D.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation
Geological Society, London, Special Publications; 1992; v. 65; p. 21-30;
DOI: 10.1144/GSL.SP.1992.065.01.03
© 1992 Geological Society of London

Sedimentology and Stratigraphic Correlation

Techniques and applications of petrophysical correlation in submarine fan environments, early Tertiary sequence, North Sea

I. R. Hatton1, M. Reeder1, M. St. J. Newman1 & D. Roberts2

1 Kerr-McGee Oil (UK) plc, 75 Davies Street, London W1Y 1FA, UK
2 ResTech Europe Ltd, 5 Red Lion Court, Off Alexander Road, Hounslow, Middlesex TW3 1JS, UK
Roberts Associates, Charnwood, Mayfield Road, Weybridge, Surrey KT13 8XB, UK

Accurate stratigraphic delineations and correlations are key factors in exploration and development of early Tertiary reservoirs of the North Sea. In the submarine fan environment, application of biostratigraphic data can be complicated by stacking of sand sequences. A sand indicator is derived from a wireline log computation. The sand intervals are then edited out to generate a log profile of the background sedimentary sequence. Additional refinement is obtained by use of cross plot analysis to define petrophysical attributes of selected stratigraphic units. An example is described where such analysis has been applied to the Balder Formation where a ‘tuff profile’ has been established. Further examples illustrate how the methods serve to extrapolate detailed biostratigraphic data of wells into adjacent wells with limited or no data.