Tectonometamophic evolution of the Greater Himalayan sequence, Karnali valley, northwestern Nepal
In the Karnali valley of west Nepal, detailed mapping, thermobarometry, quartz-petrofabrics, vorticity analysis, and thermochronology delineate three tectonometamorphic domains separated by structural and metamorphic discontinuities. The lowest domain, the Lesser Himalayan sequence, is weakly metamo...
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| Language: | en en |
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2010
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| Online Access: | http://hdl.handle.net/1974/6058 |