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The AAPG/Datapages Combined Publications Database

Journal of Petroleum Geology

Abstract

Journal of Petroleum Geology, Vol.2, No.1, pp. 75-93, 1979

©Copyright 2000 Scientific Press, Ltd.

THE GEOLOGY AND HYDROCARBON HABITAT OF THE BRISTOL CHANNEL BASIN

P. Kamerling*

* Shell U.K. Exploration and Production, Shell Centre, London SEI 7NA.


Abstract

The Bristol Channel Basin forms an early Mesozoic ((?Permo-) Triassic--Jurassic) basin development with a relatively thin cover of Cretaceous and Tertiary sediments. On the basis of structural trends and stratigraphy, the Basin can be divided into two sub-basins: the ENE-WSW trending Main Bristol Channel Basin and the E-W trending East Bristol Channel Basin. In between them there is an Intermediate Area which incorporates features of the sub-basins on either side. This subdivision appears to be the result of the presence of major NW-SE basement faults which intersect the Bristol Channel area in several places.

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