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Permo-carboniferous Magmatism and Rifting in Europe

Series: Geological Society Special Publications Volume: 223

Edited By: M Wilson, ER Neumann, GR Davies, MJ Timmerman, M Heeremans and BT Larsen

498 pages, Figs, tabs

Geological Society

Hardback | Dec 2004 | #152073 | ISBN: 1862391521
Availability: Usually dispatched within 1-2 weeks Details
NHBS Price: £159.00 $194/€179 approx

About this book

Widespread extension occurred within the Variscan orogen and its northern foreland during Late Carboniferous to Early Permian times. This was associated with magmatism and with a fundamental change, at the Westphalian-Stephanian boundary, in the regional stress field, coincident with the termination of orogenic activity and onset of dextral translation between North Africa and Europe. Rifting propagated across basement terranes with different ages and thermal histories. Most of the rift basins developed on relatively thin lithosphere; however, the highly magmatic Oslo Graben initiated within the edge of a craton. Early Stephanian regional uplift is contemporaneous with the onset of magmatism, inviting speculation that it might have been induced by a thermal anomaly within the upper mantle. The contributions to this volume suggest that the geodynamic setting in which magmatism occurred was complex, involving wrench tectonics, slab detachment, and delamination or thermal erosion of the base of the lithosphere.

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