Avouac, Jean-Philippe and Tapponnier, Paul (1993) Kinematic model of active deformation in central Asia. Geophysical Research Letters, 20 (10). pp. 895-898. ISSN 0094-8276 http://resolver.caltech.edu/CaltechAUTHORS:20120911-105620191
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The velocity field of present‐day deformation in Central Asia is modelled using a set of four rotating blocks (Siberia, Tarim, Tibet, India) on a spherical earth. A best‐fit is inverted on the basis of estimated shortening‐rates across the main thrust zones (Himalayas, Tien Shan) and measured slip‐rates along the principal strike‐slip faults (Altyn Tagh and Karakorum) separating those blocks. The fit to the data implies that nearly all the present convergence between India and Asia can be accounted for by slip‐partitioning on these four zones, with as much as 50% absorbed by northeastwards extrusion of Tibet. This suggests that localised deformation governs the present mechanical behaviour of the Central Asian lithosphere.
|Additional Information:||© 1993 American Geophysical Union. Received December 17, 1992; accepted January 7, 1993. We acknowledge support from DBT, IST, INSU and CNRS.|
|Official Citation:||Avouac, J. and P. Tapponnier (1993), Kinematic model of active deformation in central Asia, Geophys. Res. Lett., 20(10), 895–898, doi:10.1029/93GL00128.|
|Usage Policy:||No commercial reproduction, distribution, display or performance rights in this work are provided.|
|Deposited By:||Ruth Sustaita|
|Deposited On:||11 Sep 2012 18:23|
|Last Modified:||26 Dec 2012 16:08|
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