A review of the geologic history of the Himalayan-Tibetan orogen suggests that at least 1400
km of north-south shortening has been absorbed by the orogen since the onset of the Indo …

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 …

摘要青藏高原是我国现代构造活动和地震活动最强烈的地区, 自有地震记录以来,
在高原内记录到多达18 次8 级以上巨大地震和100 余次7~ 7.9 级地震, 它们均发生在喜马拉雅 …

摘要喜马拉雅2 青藏高原造山带的地质历史显示出, 自从约70Ma 印度板块2
亚洲板块开始碰撞以来, 至少有1 360 km 的SN 向缩短量被喜马拉雅2 青藏高原造山带所吸收 …

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 …

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 …

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 …

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 …

The pattern of fluvial incision across the Himalayas of central Nepal is estimated from the
distribution of Holocene and Pleistocene terraces and from the geometry of modern …

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 …