qinghai-tibet plateau uplift 青藏高原隆升
tibet plateau uplift 青藏高原隆升
qinghai xizang plateau uplift 青藏高原隆升
qinghai-xizang plateau uplift 青藏高原隆升过程
uplift plateau 高原隆升
uplift of plateau 高原隆升
uplift of Tibetan Plateau 青藏高原隆升
The continuous and periodic uplift of the Qinghai-Tibet Plateau since the Cenozoic is an important geological and environmental event during the evolution of the Earth.
青藏高原新生代以来的持续性、阶段性隆升是地球演化过程中重要的地质和环境事件。
The late Cenozoic geomorphologic and sedimentary features in the west Kunlun Mountain front record the uplift process of the west Kunlun Mountains and the western margin of the Qinghai-Tibet Plateau.
西昆仑山前晚新生代地貌与沉积特征记录了西昆仑山及青藏高原西北缘的隆升过程。
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