Despite a long research history over the past 150 years, the geometry, kinematics, and
dynamic evolution of the Himalayan orogen remain poorly understood. This is mainly due to …

Indian plate rocks in the central Himalaya have traditionally been divided into orogen‐
parallel, fault‐bound tectonostratigraphic zones. A straightforward westward extrapolation of …

The Himalayan range is one of the best documented continent-collisional belts and provides
a natural laboratory for studying subduction processes. High-pressure and ultrahigh …

Abstract The Kohistan-Ladakh block occupies the northwestern corner of the Himalayan
mountains and has long been recognized to represent an island arc constructed on ocean …

Abstract The western Himalaya of Pakistan forms a classic fold and thrust belt with a
foreland defined by the Salt Range thrust, Main Boundary thrust, and Panjal-Khairabad …

Abstract The> 2000-km-long Indus–Tsangpo suture zone (ITSZ) in southern Tibet contains
remnants of Neotethyan oceanic lithosphere, ophiolitic mélanges, flysch units and …

The major goal of this research was to explore low cost means by which large tracts of
mountainous terrain (∼ 75000 km2) can be screened for landslide-related hazards. For …

U‐Pb zircon isotopic ages of seven rock samples are combined with field data to provide
constraints on deposition, intrusion, and metamorphism in the northwestern part of the …

The China–Pakistan Economic Corridor (CPEC) project passes through the Karakoram
Highway in northern Pakistan, which is one of the most hazardous regions of the world. The …

The suture zones, which border the Indian craton in Pakistan are characterized by several
large mafic–ultramafic complexes. From south to north these include:(1) Bela,(2) …