This article summarizes recent advances in our knowledge of the past 1000 years of
earthquakes in the Himalaya using geodetic, historical and seismological data, and …

The Himalayan-Tibetan orogen culminated during the Cenozoic India--Asia collision, but its
geological framework and initial growth were fundamentally the result of multiple, previous …

Detrital thermochronology studies based on the lag-time approach are increasingly
employed to investigate the erosional evolution of mountain belts and perform paleotectonic …

We determine the slip rate and pattern of interseismic coupling on the Main Himalayan
Thrust along the entire Himalayan arc based on a compilation of geodetic, interferometric …

Competing models that account for the construction of the Tibetan Plateau include
continental subduction, underthrusting, distributed shortening, channel flow, and older …

The return times of large Himalayan earthquakes are poorly constrained. Despite historical
devastation of cities along the mountain range, definitive links between events and specific …

GPS data reveal that the Brahmaputra Valley has broken from the Indian Plate and rotates
clockwise relative to India about a point a few hundred kilometers west of the Shillong …

In this study, we present a new synthesis of GPS velocities for tectonic deformation within the
Tibetan Plateau and its surrounding areas, a combined data set of∼ 1854 GPS-derived …

Abstract The Cenozoic Qilian Shan thrust belt is the northern margin of the Tibetan Plateau,
which developed in part due to progressive India-Asia convergence during Himalayan …

Abstract The Bengal Basin is a collisional foreland basin in South Asia located at the
juncture of the Eurasian, Indian and Burmese Plates occupying Bangladesh and parts of the …