Geological history of Britain and Ireland by Nigel H. Woodcock, R. A. Strachan

By Nigel H. Woodcock, R. A. Strachan

Britain and eire have a remarkably diverse geology for therefore small a fraction of continental crust, with a superb rock checklist again via 3 billion years of geological time. This heritage could were attention-grabbing sufficient if it were performed out on fairly good continental crust. even if, Britain and eire have built at a tectonic crossroads, on crust as soon as traversed via subduction zones and volcanic arcs, continental rifts and mountain belts. The ensuing complexity is instructive, attention-grabbing and perplexing.
Geological historical past of england and eire tells the region's tale at a degree available to undergraduate geologists, in addition to to postgraduates, pros or trained amateurs. This moment version is absolutely revised and up-to-date, reflecting our regularly constructing wisdom of the region's geology. complete insurance is back given to the wealthy Precambrian and Early Palaeozoic background, in addition to to later occasions extra appropriate to hydrocarbon exploration. The ebook is a necessary place to begin for extra specified reviews of the neighborhood geology.

Additional assets for this e-book are available at http://www.wiley.com/go/woodcock/geologicalhistory

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Additional resources for Geological history of Britain and Ireland

Example text

A Variscan deformation front separates the strongly deformed zone from the area to the north, in which the post-Acadian cover was only gently deformed (Fig. 9b). By early Permian time, the crust of Britain and Ireland had been assembled in more or less its present configuration. The post-Variscan cycle (Part 6) is dominated by sediment accumulation in basins formed by crustal extension, attributable to the marginal effects of the rifting and opening of the Atlantic Ocean. The pulsed nature of extension has produced gentle unconformities (such as the Cimmerian, Fig.

The assembly of Pangaea, for example, did not follow the extroversion model (see Fig. 6). The break-up of Pannotia in the latest Neoproterozoic–early Cambrian led to the separation of Laurentia, Baltica and Gondwana due to the opening of new interior oceans such as the Iapetus and the Rheic. Had this process continued following the extroversion model, the continents should have migrated towards the subduction zones at the margins of the surrounding palaeo-Pacific, leading ultimately to the destruction of that ocean.

2012 Blackwell Publishing Ltd. Published 2012 by Blackwell Publishing Ltd. 20 Geological Framework of Britain and Ireland Fig. 1 Parameters of global change through Phanerozoic time: (a) number of major continents; (b) rate of intrusion of North American granites; (c) global sea level; (d) atmospheric concentration of carbon dioxide; (e) atmospheric concentration of oxygen; (f) global average surface temperature; (g) number of genera in representative groups of organisms, subdivided into component faunas, and showing percentage species loss in major mass extinctions (data from Phillips & Bunge 2007 (a), Veevers 1990 (b); Haq & Al-Qahtani 2005 (c); Royer et al.

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