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- Sensitivity of the East Asian Monsoon Climate to the Tibetan Plateau Uplift 东亚季风气候对青藏高原隆升的敏感性研究
- TIBETAN PLATEAU UPLIFT AND DRYING IN EURASIAN INTERIOR AND NORTHERN ARFICA 青藏高原隆升与欧亚内陆及北非的干旱化
- Tibetan plateau uplift 青藏高原隆升
- Geological Evidences for the Tibetan Plateau Uplifted in Late Oligocene 青藏高原渐新世晚期隆升的地质证据
- We concentrate on introducing the progress of the study on mantle dynamic mechanism of the uplift of Tibetan Plateau. 并重点评述在青藏高原隆升的地幔动力学机制研究领域所取得的主要结果。
- The uplift and formation of the Tibetan Plateau is the dynamic consequence of the collision between the Indian and Eurasian plates. 摘要青藏高原的形成是印度板块与欧亚大陆碰撞、挤压的结果,但简单的碰撞模型及南西-北东向的挤压无法解释高原现今所有的构造。
- The late Cenozoic uplift of the Tibetan Plateau played a great role in the geomorphic and depositional evolution of its adjacent areas. 晚新生代青藏高原的隆升对其周围地貌格局和沉积产生了重大影响。
- The evolution of the depositional environment and migration of the depocenter could be affected by early uplift of the Tibetan plateau. 这种沉积环境演化和盆地沉积中心迁移可能受青藏高原早期隆升的影响。
- It draws pilgrims from across the Tibetan plateau. 它吸引着来自青藏高原的众多香客。
- The Oligo-Miocene paleoclimate and tectonic evolution of the Wuyu Basin has displayed its significance for understanding the early uplift of the Tibetan Plateau. 乌郁盆地渐新世-早更新世沉积相分析对于研究青藏高原隆升和油气等能源均具有重要意义。
- Xiyu Formation is characterized by coarse debris flow deposits,marking the strong uplift of the northern part of Tibetan Plateau and unroofing of the West Kunlun. 西域组的沉积标志着作为物源区的西昆仑山已有相当的高度。
- Designing idea : The inspiration comes from the Tibetan Plateau. 设计构思:灵感来于雪域高原的那圣洁的雪山,鲜红的藏饰。
- LI Hai-bing. 2001.Formation Era of Altyn Tagh Fault Zone and Contribution of its Strike-Slip to the Uplift of North Tibetan Plateau [D].Ph D thesis.Institute of Geology, CAGS, Beijing (in Chinese). 李海兵.;2001
- The yankees closed shells and instructions of qinghai-tibet plateau uplift period intracontinental orogenic movement of magmatic activity. 指示洋壳闭合后,青藏高原隆升期的陆内造山运动中的岩浆活动。
- Since the beginning of the Quaternary, with the uplift of Tibetan Plateau, the Asian monsoon was established and became the controlling factor of the climate and environmental change of China. 自第四纪以来,青藏高原的隆升以及因此而建立起来的东亚季风季风系统成为我国气候、环境的最主要控制因素。
- Estimation of Land Surface Temperature over the Tibetan Plateau Using GMS Data. 用GMS数据估计青藏高原陆地表面温度。
- Fabled Land: The train from Golmud to Lhasa reaches the Tibetan plateau. 传奇的土地:这列从格尔木到拉萨的火车到达西藏高原。
- Lakes developed widely during Cenozoic era in central Tibetan Plateau. 青藏高原中部新生代湖泊发育普遍。
- The results indicate that Qinghai-Tibet plateau uplift have arose multi-geological hazards, and the uplift of loess plateau have induced gravitative, trace to the source and water-flow erosion. 结果表明,青藏高原的隆升引起多种黄土地质灾害。黄土高原的构造抬升导致侵蚀基准面下降,为重力侵蚀、沟谷溯源侵蚀和流水侵蚀提供了有利条件;
- This article pointed out that the distributing pattern of Chinese desert and desertification is V shapesd, and the Qinghai-Tibet plateau uplift may be the main factor to this pattern. 本文指出,中国沙漠与沙漠化分布呈“V”型格局,而青藏高原的隆起对中国沙漠与沙漠化格局的形成具有决定性的作用。