The timing of initial collision between India and Asia has remained controversial for half a
century. This paper attempts to review this crucial and hotly debated argument, describing …

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 …

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 …

摘要通过广泛的野外地质调查和岩石地球化学, 矿床学, Re-Os 同位素, 硫, 铅同位素的综合研究,
首次比较系统地论述了雅鲁藏布江北侧冈底斯斑岩型铜矿带含矿斑岩的岩石地球化学特征和 …

On multimillion-year time scales, Earth has experienced warm ice-free and cold glacial
climates, but it is unknown whether transitions between these background climate states …

Weathering profiles developed on basalt substrate contain information relevant to climate,
atmospheric composition and evolution, nutrient release into the hydrosphere, and …

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 …

During the Mesozoic–Cenozoic, northward Neotethyan subduction and subsequent India–
Asia collision gave rise to the extensive Transhimalayan magmatism that stretches from …