The metamorphism and exhumation of the Himalayan metamorphic core, eastern Garhwal region, India
[1] Geothermobarometric together with micro- and macro-structural data indicate ductile flow in the metamorphic core of the Himalaya in the Garhwal region of India. Peak metamorphic pressure and temperature increase dramatically across the Main Central Thrust (MCT) from ~5 kbar and ~550°C in the Les...
| Main Authors: | , , |
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| Format: | Journal Article |
| Published: |
American Geophysical Union
2012
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| Online Access: | http://hdl.handle.net/20.500.11937/3480 |