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Himalayan tectonics explained by extrusion of a low-viscosity crustal channel coupled to focused surface denudation

GeophysicsRift SystemIndia-asia Collision ZoneFocused Surface DenudationHimalayan TectonicsEngineeringPlate BoundaryGeomorphologyGeographyIndia-asia CollisionGeologyLow-viscosity Crustal ChannelOrogenyEarth ScienceTectonics