By J. R. Underhill
The Wessex Basin is volumetrically an important united kingdom onshore petroleum province. This ebook makes use of not just floor outcrops but in addition details supplied by means of subsurface information, principally received within the winning quest for advertisement hydrocarbons, to supply insights into the improvement, evolution and petroleum geology of the Wessex Basin. additionally to be had: The Geology of britain And Wales - ISBN 1862391998 Key matters 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 greatest publishers within the Earth sciences.The Society publishes a variety of top quality peer-reviewed titles for teachers and execs operating within the geosciences, and enjoys an enviable foreign acceptance for the standard of its work.The many components during which we submit in include:-Petroleum geology-Tectonics, structural geology and geodynamics-Stratigraphy, sedimentology and paleontology-Volcanology, magmatic stories and geochemistry-Remote sensing-History of geology-Regional geology courses
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Additional resources for The Development, evolution and petroleum geology of the Wessex Basin
Arkell International Symposium. The Jurassic of Dorset Excursion Guide. University College, London. CHADWICK, R. A. 1985a. Permian, Mesozoic and Cenozoic structural evolution of England and Wales in relation to the principles of extension and inversion tectonics. In: WHITTAKER, A. ) Atlas of Onshore Sedimentary Basins in England and Wales: Post-Carboniferous Tectonics and Stratigraphy. Blackie, Glasgow, 9-25. - - 1 9 8 5 b . Cenozoic sedimentation, subsidence and basin inversion. In: WHITTAKER, A.
Ll. Gross isopach map for the Early Jurassic Lias Group showing the importance that some extensional faults had in controlling thickness variation. unconformity at the top of the Junction Bed of Toarcian age (Fig. 4). The top of the J2 sequence is marked by the Inferior Oolite in both the Wessex and Weald basins. It is fairly well developed in the sediment-starved Weald, but is thin and sometimes difficult to identify above the Bridport Sands in the Wessex Basin. The Bridport Sands (Figs 13 15) form an important reservoir horizon in the Wessex Basin.
1969. International Field Symposium on the British Jurassic. Excursion No. 1, Guide for Dorset and South Somerset. University of Keele, A l-A71. UNDERHILL, J. R. & PATERSON, S. 1998. Genesis of tectonic inversion structures: seismic evidence for the development of key structures along the Purbeck-Isle of Wight Disturbance. Journal of the Geological Society, London, in press. STONELEY, R. 1998. Introduction to the development, evolution and petroleum geology of the Wessex basin. This volume. , WELCH, F.