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

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

Mineralogical and fluid inclusion constraints on the formation of

Enigmatic C' shear bands: their evolution and demise

Observed intensity distribution for the 1897 Assam earthquake (1a

Spatial and Temporal Distributions of Deformation in Strike-Slip Faults: The Karakoram Fault in the India-Asia Collision Zone - ScienceDirect

PDF) Twenty million years of continous deformation along the

Evolution of the Eastern Karakoram Metamorphic Complex, Ladakh, NW

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

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

Vol 45 Spe, PDF, Himalayas

PDF) Deformation fabrics and strain localization mechanisms in

Spatial and Temporal Distributions of Deformation in Strike-Slip Faults: The Karakoram Fault in the India-Asia Collision Zone - ScienceDirect

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

Map showing location and felt time in minutes of Kangra aftershocks.

Digital elevation map of the Tibetan Plateau region showing active