Estimation of deformation temperatures, flow stresses and strain rates from an intra-continental shear zone: The Main Boundary Thrust, NW Himalaya (Uttarakhand, India)

Author:

Bose NarayanORCID,Mukherjee Soumyajit

Funder

IIT Bombay

Publisher

Elsevier BV

Subject

Stratigraphy,Economic Geology,Geology,Geophysics,Oceanography

Reference170 articles.

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2. Convergence rate across the Nepal Himalaya and interseismic coupling on the main Himalayan thrust: implications for seismic hazard;Ader;J. Geophys. Res.: Solid Earth 117B04403,2012

3. Shear-zone geometries in experimentally deformed clays: the influence of water content, strain rate and primary fabric;Arch;J. Struct. Geol.,1988

4. The microstructural and rheological evolution of shear zones;Austin,2011

5. Syntectonic vein development in a thrust sheet from the external French Alps;Beach;Tectonophysics,1982

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