P Tapponnier, X Zhiqin, F Roger, B Meyer, N Arnaud… - science, 2001 - science.org
Two end member models of how the high elevations in Tibet formed are (i) continuous thickening and widespread viscous flow of the crust and mantle of the entire plateau and (ii) …
Sundaland, the continental core of SE Asia, is a heterogeneous collage of continental blocks and volcanic arcs bounded by narrow suture zones that represent the remnants of ancient …
We document geodetic strain across the Nepal Himalaya using GPS times series from 30 stations in Nepal and southern Tibet, in addition to previously published campaign GPS …
Despite a long research history over the past 150 years, the geometry, kinematics, and dynamic evolution of the Himalayan orogen remain poorly understood. This is mainly due to …
J Huang, D Zhao - Journal of Geophysical Research: Solid …, 2006 - Wiley Online Library
A high‐resolution P wave tomographic model of the crust and mantle down to 1100 km depth under China and surrounding regions is determined by using about one million arrival …
KV Hodges - Geological Society of America Bulletin, 2000 - pubs.geoscienceworld.org
Abstract The Himalaya and Tibet provide an unparalleled opportunity to examine the complex ways in which continents respond to collisional orogenesis. This paper is an …
KD Nelson, W Zhao, LD Brown, J Kuo, J Che, X Liu… - science, 1996 - science.org
INDEPTH geophysical and geological observations imply that a partially molten midcrustal layer exists beneath southern Tibet. This partially molten layer has been produced by crustal …
We analyze geomorphic evidence of recent crustal deformation in the sub‐Himalaya of central Nepal, south of the Kathmandu Basin. The Main Frontal Thrust fault (MFT), which …