Widespread anatexis was a regional response to the evolution of the Himalayan‐Tibetan
Orogen that occurred some 30 Ma after collision between Asia and India. This paper reviews …

Crustal shortening and thickening to c. 70–85 km in the Tibetan Plateau occurred both
before and mainly after the c. 50 Ma India–Asia collision. Potassic–ultrapotassic shoshonitic …

Abstract The India‐Eurasia collision zone is the largest deforming region on the planet;
direct measurements of present‐day deformation from Global Positioning System (GPS) …

Asia has been a major testing ground for various competing models of continental
deformation due to its relatively well-understood plate boundary conditions in the Cenozoic …

A long‐standing problem in the geological evolution of the India‐Asia collision zone is how
and where convergence between India and Asia was accommodated since collision …

New detrital zircon and isotopic (Nd and Sr) analyses from the eastern Pamir provide
information on the depositional age and tectonic terrane affiliation of regional metamorphic …

The northern part of the Pamir orogen is the preeminent example of an active
intracontinental subduction zone in the early stages of continent–continent collision. Such …

The timing of the late Cenozoic collision between the Pamir salient and the Tien Shan as
well as changes in the relative motion between the Pamir and Tarim are poorly constrained …

The northeast Cathaysia area is characterized by an archetypical, transpressional system
with widespread strike‐slip shear zones whose geometries, kinematics, and ages are critical …

We investigate the timing of end of motion along the South Tibet Detachment System
(STDS), a major normal fault system that runs parallel to the Himalayan range for more than …