Shear structures in the Kohistan arc

Shear band developed in strongly sheared Kohistan arc rocks.
Shear band developed in strongly sheared Kohistan arc rocks (with deformed Confluence granite sheets).  These may be used to deduce the sense of shear along the early ductile contact between Kohistan and Nanga Parbat rocks.

Looking west along the Indus River.  The boulders on the left are up to 2m across.