western qinghai-tibet plateau

基本解释

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.
川青地块在地貌上为川西高原，亦是青藏高原东北边缘最重要的构造单元。
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.
青海位于青藏高原东北部、泛华夏陆块群的中西部，东特提斯的北部。
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。