Download The Development, evolution and petroleum geology of the by J. R. Underhill PDF

By J. R. Underhill

ISBN-10: 1897799993

ISBN-13: 9781897799994

The Wessex Basin is volumetrically crucial united kingdom onshore petroleum province. This publication makes use of not just floor outcrops but additionally info supplied through subsurface facts, mostly bought within the profitable quest for advertisement hydrocarbons, to supply insights into the improvement, evolution and petroleum geology of the Wessex Basin. additionally on hand: The Geology of britain And Wales - ISBN 1862391998 Key concerns in Petroleum Geology - Stratigraphy (Key matters in Earth Sciences) - ISBN 1862392374 The Geological Society of LondonFounded in 1807, the Geological Society of London is the oldest geological society on this planet, and one of many biggest publishers within the Earth sciences.The Society publishes quite a lot of top quality peer-reviewed titles for teachers and execs operating within the geosciences, and enjoys an enviable overseas popularity for the standard of its work.The many components during which we post in include:-Petroleum geology-Tectonics, structural geology and geodynamics-Stratigraphy, sedimentology and paleontology-Volcanology, magmatic reports and geochemistry-Remote sensing-History of geology-Regional geology courses

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Additional info for The Development, evolution and petroleum geology of the Wessex Basin

Example text

Full preservation of this sequence in the Wessex Basin is limited to the hanging wall Fig. 19. Gross isopach map for the Corallian showing the continued role that extensional faults had in controlling deposition. 56 P. W. HAWKES ET AL. Fig. 20. Lithofacies map for the Corallian showing the limits of carbonate and clastic deposition in the Weald and Wessex basins. of faults active during the Lower Cretaceous rifting event associated with opening of the Bay of Biscay. Biscay plate sequence During the Early Cretaceous the Weald and Wessex (Portland-South Wight) basins were subject to a phase of major renewed extension, probably associated with active rifting along the Biscay continental margin (Fig.

The Varsican orogeny imparted a strong east-west (thrusts) and northwest-southeast (lateral transfers) structural grain across the province. In the area of the present-day Western Approaches the east-west trends swing round 9into a more northeast-southwest direction. During subsequent Permian and Mesozoic rifting and inversion, Variscan trends were periodically reactivated in an extensional or compressional sense (Chadwick et al. 1983). A similar reactivation of Caledonian collisional grain during Carboniferous rifting and inversion was noted by Fraser et al.

Inversion movements on the old extensional faults led to the development of hanging wall anticlines which rely upon remigration mechanisms, including exsolution of gas from uplifted Liassic source rocks, to receive hydrocarbon charge. To date over 300 million barrels of oil and 100 bcf of gas have been discovered. This paper describes the results of a major regional study carried out at BP Exploration's U K land offices in Eakring during the late 1980s. At that time BP had amassed a substantial database of modern well and seismic data in addition to the results of exploration activity dating back to the 1930s.

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