The surface uplift history of the Tibetan Plateau (TP) offers a key testing ground for
evaluating models of collisional tectonics and holds important implications for processes …

Recent studies of the northeastern part of the Tibetan Plateau have called attention to two
emerging views of how the Tibetan Plateau has grown. First, deformation in northern Tibet …

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 …

Reconstructing the Paleogene topography and climate of central Tibet informs
understanding of collisional tectonic mechanisms and their links to climate and biodiversity …

The onset of mountain building along margins of the Tibetan Plateau provides a key
constraint on the processes by which the high topography in Eurasia formed. Although …

Abstract The India‐Eurasia collision zone is the largest deforming region on the planet;
direct measurements of present‐day deformation from Global Positioning System (GPS) …

青藏东南缘是青藏高原物质东流的通道, 为了更全面了解复杂的岩石圈结构和强烈的变形特征,
本文介绍了青藏东南缘岩石圈各向异性的形态, 综合其他研究者得到的该区域壳幔各向异性结果 …

Competing geodynamic models, such as rigid-block extrusion, continuous deformation, and
the mid-lower crustal flow, have been proposed to describe the growth and expansion of …

The appearance of detritus shed from mountain ranges along the northern margin of the
Tibetan Plateau heralds the Cenozoic development of high topography. Current estimates of …