The Nanga Parbat-Haramosh massif (NPHM) is a north-south trending
structural and topographic high, which interrupts the east-west trend
of the Himalaya in northern Pakistan. Previously, the massif was
thought to be bounded by the Main Mantle thrust (MMT), a north-dipping
thrust along which the Kohistan-Ladakh arc was thrust south over...
The Himalaya are the geologic manifestation of continental collision,
and in northern Pakistan the Main Mantle thrust (MMT) is a major suture along
which the collision occurred. A newly recognized basement uplift near
Besham village in southern Kohistan, adjacent to the MMT, is bounded on the
east and west by...
