Deformation fabrics on the Nubra fault strand. (a–c): Nubra Formation

Tomographic image of Pn velocity anisotropy. Line segments are drawn

Low effective fault strength due to frictional-viscous flow in phyllonites, Karakoram Fault Zone, NW India - ScienceDirect

PDF) Fault weakening across the frictional-viscous transition zone, Karakoram Fault Zone, NW Himalaya

Cartoon illustrating the generation of post-critical SmS arrivals. If

Petrology, geochemistry and geochronology of granites and granite gneisses in the SE Karakoram, India: Record of subduction-related and pre- to syn-kinematic magmatism in the Karakoram Fault Zone

Digital elevation map of the Tibetan Plateau region showing active

PDF) Low effective fault strength due to frictional-viscous flow in phyllonites, Karakoram Fault Zone, NW India

PDF) Fault weakening across the frictional-viscous transition zone, Karakoram Fault Zone, NW Himalaya

Richard PHILLIPS, University of Leeds, Leeds, Institute of Geophysics and Tectonics (IGT)

Interplay of deformation and magmatism in the Pangong

PDF) Fault weakening across the frictional-viscous transition zone, Karakoram Fault Zone, NW Himalaya

A) Photomicrograph showing oscillatory zoning in plagioclase