青藏高原新生代伸展地堑构造是高原经历早期地壳强烈缩短变形之后，在深部动力学机制作用下快速隆升的产物。
The Cenozoic extensional grabens on the Qinghai-Tibet plateau are the product of rapid uplift of the plateau caused by the deep dynamic mechanism after earlier strong crustal shortening.
青藏高原新生代伸展地堑构造是高原经历早期地壳强烈缩短变形之后，在深部动力学机制作用下快速隆升的产物。
The Cenozoic extensional grabens on the Qinghai-Tibet plateau are the product of rapid uplift of the plateau caused by the deep dynamic mechanism after earlier strong crustal shortening.
应用推荐