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青藏高原是研究陆陆碰撞的关键地区,高原在晚新生代以来的隆起及其对自然环境的影响是我国有特色的优势研究领域,在国际上竞争激烈。根据科学发展的趋势和前沿领域,本文概述了大陆碰撞变形与过程,高原岩石圈结构特征,高原形成演化模式,高原隆升过程的争论,高原隆升与东亚环境变化以及2000年来气候环境变化等方面的主要研究进展。
The Qinghai-Tibet Plateau is a key area for studying land-continent collisions. The uplift of the plateau since the Late Cenozoic and its impact on the natural environment are the unique research areas for our country’s advantage. They are highly competitive internationally. According to the trend of scientific development and frontier fields, this paper summarizes the continental collision deformation and process, the plateau lithospheric structure, the plateau formation and evolution, the plateau uplift, the uplift of the plateau and the change of East Asia and the climate change in 2000 The main research progress.