crustal dynamics

基本解释

The Sichuan-Yunnan area is an ideal area for studying tectonic movement and its crustal dynamics problem of continent.
川滇地区是大陆构造运动及其动力学过程研究的理想的实验场地。
Therefore, the elastic wave velocity and dynamics on crustal and mantle rocks at much higher PT should be further studied.
因此，有必要在更高的温压条件下对弹性波通过壳幔岩石的速度和动力学特征等方面进行深入研究。
This research constrains the orogeny of Mongolian-Okhotsk belt and is beneficial to discussion on the Jurassic crustal tectonic evolution of NE China and dynamics of the Yanshan movement.
这一研究成果，对蒙古-鄂霍茨克造山带的造山作用过程给予了约束，也有助于揭示中国东北地区侏罗纪地壳演化和燕山运动的动力学机制。