Tectonics of the Himalaya

Tectonics of the Himalaya

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The Himalayan mountain belt, which developed during the Indiaa€“Asia collision starting about 55 Ma ago, is a dramatically active orogen and it is regarded as the classic collisional orogen. It is characterized by an impressively continuous 2500 km of tectonic units, thrusts and normal faults, as well as large volumes of high-grade metamorphic rocks and granites exposed at the surface. This constitutes an invaluable field laboratory, where amazing crustal sections can be observed directly in very deep gorges. It is possible to unravel the tectonic and metamorphic evolution of litho-units, to observe the mechanisms of exhumation of deep-seated rocks and the propagation of the deformation. Himalayan tectonics has been the target of many studies from numerous international researchers over the years. In the last 15 years there has been an explosion of data and theories from both geological and geophysical perspectives. This book presents the results of integrated multidisciplinary studies, including geology, petrology, magmatism, geochemistry, geochronology and geophysics, of the structures and processes affecting the continental lithosphere. These processes and their spatial and temporal evolution have major consequences on the geometry and kinematics of the Indiaa€“Eurasia collision zone.The Debon aamp; Le Fort diagram (Debon et al. ... The 1997 HimlungHimal CAF expedition, with S. Guillot, was his last field mission, resulting in publication of the cartography of the ... In: COWARDS, M. P. aamp; RIES, A. C. (eds) Collision Tectonics.

Title:Tectonics of the Himalaya
Author: S. Mukherjee, R. Carosi, P.A. van der Beek, B.K. Mukherjee, D.M. Robinson
Publisher:Geological Society of London - 2015-09-28

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