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Sean Long et al.
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The Malari leucogranite, Garhwal Himalaya, northern India: Chemistry, age, and tectonic implications
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P-T Evolution across the Main Central Thrust Zone (Eastern Nepal): Hidden Discontinuities Revealed by Petrology
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Pre-Miocene deformation of the Himalayan superstructure, Hidden valley, central Nepal
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P-T-t data from central Nepal support critical taper and repudiate large-scale channel flow of the Greater Himalayan Sequence
Matthew J. Kohn
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Orogen-parallel extension and exhumation enhanced by denudation in the trans-Himalayan Arun River gorge, Ama Drime Massif, Tibet-Nepal
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Nigel Harris
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Formation of a high-temperature metamorphic complex due to pervasive melt migration in the hot crust
Kazuhiro Miyazaki
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The texture and composition of tourmaline in metasediments of the Sinai, Egypt: Implications for the tectono-metamorphic evolution of the Pan-African basement
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Tectonic evolution of the Himalayan thrust belt in western Nepal: Implications for channel flow models
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GEOLOGICAL SOCIETY OF AMERICA BULLETIN (2006)
Active tectonics in Eastern Lunana (NW Bhutan):: Implications for the seismic and glacial hazard potential of the Bhutan Himalaya
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Cenozoic tectonic evolution of the Himalayan orogen as constrained by along-strike variation of structural geometry, exhumation history, and foreland sedimentation
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EARTH-SCIENCE REVIEWS (2006)
Are turtleback fault surfaces common structural elements of highly extended terranes?
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EARTH-SCIENCE REVIEWS (2005)
Five generations of monazite in Langtang gneisses: implications for chronology of the Himalayan metamorphic core
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Miocene to Holocene exhumation of metamorphic crustal wedges in the NW Himalaya: Evidence for tectonic extrusion coupled to fluvial erosion
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Crustal channel flows: 1. Numerical models with applications to the tectonics of the Himalayan-Tibetan orogen
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The South Tibetan Detachment and the Manaslu Leucogranite: A structural reinterpretation and restoration of the Annapurna-Manaslu Himalaya, Nepal
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Exhumation of the Main Central Thrust from lower crustal depths, Eastern Bhutan Himalaya
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The eastern Tonale fault zone: a 'natural laboratory' for crystal plastic deformation of quartz over a temperature range from 250 to 700 degrees C
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Himalayan tectonics explained by extrusion of a low-viscosity crustal channel coupled to focused surface denudation
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Geochronologic and thermobarometric constraints on the evolution of the Main Central Thrust, central Nepal Himalaya
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Himalayan inverted metamorphism and syn-convergence extension as a consequence of a general shear extrusion
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High-precision geothermobarometry across the High Himalayan metamorphic sequence, Langtang Valley, Nepal
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