The surface uplift history of the Tibetan Plateau (TP) offers a key testing ground for
evaluating models of collisional tectonics and holds important implications for processes …

PECUBE is a three-dimensional thermal–kinematic code capable of solving the heat
production–diffusion–advection equation under a temporally varying surface boundary …

We use common conversion point (CCP) stacking of Ps receiver functions to image the
crustal structure and Moho of the Garhwal Himalaya of India. Our seismic array of 21 …

In order to understand how orogens “work,” a quantitative approach demonstrating proof of
concept is essential. Our goal is to reconcile the diverse array of tectonic features observed …

A major question about the Himalaya remains open: does a great earthquake (like the Mw~
8.1 1934 earthquake) release all the strain stored by the Tibet–India convergence during the …

Out-of-sequence deformation in the Himalaya has been caused mainly by thrusting. Out-of-
sequence thrusts, usually north-to NE-dipping foreshear planes, occur inside the Sub …

Himalayan rivers transport around a gigaton of sediment annually to ocean basins.
Mountain valleys are an important component of this routing system: storage in these valleys …

In the last decade growing interest has emerged in quantifying the spatial and temporal
variations in mountain building. Until recently, insufficient data have been available to …

The Himalaya is the result of the on-going convergence and collision of India and Asia. The
internal configuration and processes that govern the rise of the Himalayan Mountains and …

Both climatic and tectonic processes affect bedrock erosion and exhumation in convergent
orogens, but determining their respective influence is difficult. A requisite first step is to …