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

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

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

Interplay of deformation and magmatism in the Pangong

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

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

Interplay of deformation and magmatism in the Pangong

PDF] Micro-geodynamics of the Karakoram Fault Zone, Ladakh, NW Himalaya

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

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

Geoffrey E. Lloyd's research works University of Leeds, Leeds and other places

Geoffrey E. Lloyd's research works University of Leeds, Leeds and other places

Age constraints on ductile deformation and long-term slip rates

Mineralogical and fluid inclusion constraints on the formation of the Karakorum Migmatite: implications for H2O-fluxed melting and exhumation of the South Tibetan Crust

Interplay of deformation and magmatism in the Pangong

PDF) Deformation fabrics and strain localization mechanisms in graphitic carbon-bearing rocks from the Ailaoshan-Red River strike-slip fault zone

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