Dynamic topography produced by lower crustal flow against rheological strength heterogeneities bordering the Tibetan Plateau
Author:
Publisher
Oxford University Press (OUP)
Subject
Geochemistry and Petrology,Geophysics
Link
http://academic.oup.com/gji/article-pdf/162/2/575/5963287/162-2-575.pdf
Reference52 articles.
1. Himalayan tectonics explained by extrusion of a low-viscosity crustal channel coupled to focused surface denudation;Beaumont;Nature,2001
2. Lateral extrusion of lower crust from under high topography, in the isostatic limit;Bird;J. geophys. Res.,1991
3. Core complex geometries and regional scale flow in the lower crust;Block;Tectonics,1990
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