Was Late Cretaceous–Palaeocene obduction of ophiolite complexes the primary cause of crustal thickening and regional metamorphism in the Pakistan Himalaya?

Searle, M. P. and Treloar, P. J. (2010) Was Late Cretaceous–Palaeocene obduction of ophiolite complexes the primary cause of crustal thickening and regional metamorphism in the Pakistan Himalaya? In: Kusky, T. M. , Zhai, M.-G. and Xiao, W., (eds.) The evolving continents: understanding processes of continental growth. London, U.K. : Geological Society. pp. 345-359. (Geological Society Special Publications, no. 338) ISSN (print) 0305-8719 ISBN 9781862393035

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Item Type: Book Section
Uncontrolled Keywords: geodynamics, crustal processes
Research Area: Earth systems and environmental sciences
Faculty, School or Research Centre: Faculty of Science (until 2011) > School of Geography, Geology and Environment
Depositing User: Maren Schroeder
Date Deposited: 18 Dec 2012 13:34
Last Modified: 22 Aug 2017 10:37
URI: http://eprints.kingston.ac.uk/id/eprint/24312

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