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 …

The sediment archive, of material eroded from an active tectonic region and stored in
adjacent basins, can provide a valuable record of hinterland tectonism especially when …

内容提要: 印度亚洲碰撞是新生代地球上最为壮观的重大地质事件. 碰撞及碰撞以来,
青藏高原的广大地域发生了与碰撞前截然不同的变形, 地貌, 环境及其深部结构都发生了深刻地 …

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 …

Abstract Recent interpretations of Himalayan–Tibetan tectonics have proposed that channel
flow in the middle to lower crust can explain outward growth of the Tibetan plateau,,, and that …

Within the Himalayan collisional belt, granotoids occur along two sub-parallel belts, the
Northern Himalayan Gneiss Domes (NHGD) and the High Himalayan Crystalline Series …

近10 年来," 大陆构造与动力学实验室" 在青藏高原大陆动力学研究, 尤其在特提斯演化和青藏
高原生长方面取得若干进展, 包括(1)" 青藏高原——造山的高原" 理念的提出;(2) …

Understanding the geotectonic evolution of the southeastern Tibetan plateau requires
knowledge about the structure of the lithosphere. Using data from 77 broadband stations in …

Recent research in the Himalayan fold‐thrust belt provides two new sets of observations that
are crucial to understanding the evolution of the Himalayan‐Tibetan orogenic system. First …

The Cenozoic collision between the Indian and Asian continents formed the Tibetan plateau,
beginning about 70 million years ago. Since this time, at least 1,400 km of convergence has …