Simple physical arguments, analogue experiments and numerical experiments all suggest
that the internal dynamics of actively deforming collisional mountain ranges are influenced …

This paper introduces how crustal thickening controls the growth of the Himalaya by
summarizing the P‐T‐t evolution of the Himalayan metamorphic core. The Himalayan …

Abstract Recent interpretations of Himalayan–Tibetan tectonics have proposed that channel
flow in the middle to lower crust can explain outward growth of the Tibetan plateau,,, and that …

We have compiled the distribution of active faults and folds in the Himalayan-Tibetan orogen
and its immediate surrounding regions into a web-based digital map. The main product of …

The Himalayan range exposes a spectacular assemblage of metamorphic rocks from the
mid-and deep crust that have fostered numerous models of how the crust responds to …

The channel flow model aims to explain features common to metamorphic hinterlands of
some collisional orogens, notably along the Himalaya–Tibet system. Channel flow describes …

The sediment archive, of material eroded from an active tectonic region and stored in
adjacent basins, can provide a valuable record of hinterland tectonism especially when …

Results from a thermal‐mechanical model (HT1) that includes midcrustal channel flow are
compatible with many features of the Himalayan‐Tibetan system. Radioactive self‐heating …

We analyze the Mw7. 6 Kashmir earthquake of October 8, 2005, using sub-pixel correlation
of ASTER images to measure ground deformation, and modeling seismic waveforms. The …

Abstract The late Cenozoic Kongur Shan extensional system lies along the northeastern
margin of the Pamir at the western end of the Himalayan-Tibetan orogen, accommodating …