Uplift of the Himalaya and Tibetan Plateau (HTP) and its linkage with the evolution of the
Asian monsoon has been regarded as a typical example of a tectonic–climate linkage …

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

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 …

Two end‐member kinematic models of crustal shortening across the Himalaya are currently
debated: one assumes localized thrusting along a single major thrust fault, the Main …

This article presents (U‐Th)/He thermochronological data from the Longmen Shan belt,
eastern Tibet. Located between the Songpan‐Garze terrane and the Yangtze craton, this …

In active mountain belts with steep terrain, bedrock landsliding is a major erosional agent. In
the Himalayas, landsliding is driven by annual hydro-meteorological forcing due to the …

Current theories regarding the connections and feedbacks between surface and tectonic
processes are predicated on the assumption that higher rainfall causes more rapid erosion …

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 …

This study investigates the influence of fault geometry, kinematics, and displacement on the
exhumation history of the central Himalaya using geologic mapping constraints, a new …

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 …