western qinghai-tibet plateau

基本解釋

The Sichuan-Qinghai block, which is geomorphologically the Western Sichuan Plateau, is the most important tectonic unit on the northeastern margin of the Qinghai-Tibet Plateau.
川青地塊在地貌上爲(wèi)川西高原，亦是青藏高原東北邊緣最重要的搆造單元。
Qinghai is geographically located in northeastern Qinghai-Tibet Plateau and tectonically in the mid-western part of the Pan-Cathysian Block Group and the north part of eastern Tethys.
青海位於青藏高原東北部、泛華夏陸塊群的中西部，東特提斯的北部。
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.
西崑侖山前晚新生代地貌與沉積特征記錄了西崑侖山及青藏高原西北緣的隆陞過(guò)程。