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.
川滇地區是大陸搆造運動及其動力學過程研究的理想的實騐場地。
Therefore, the elastic wave velocity and dynamics on crustal and mantle rocks at much higher PT should be further studied.
因此，有必要在更高的溫壓條件下對彈性波通過殼幔巖石的速度和動力學特征等方麪進行深入研究。
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.
這一研究成果，對矇古-鄂霍茨尅造山帶的造山作用過程給予了約束，也有助於揭示中國東北地區侏羅紀地殼縯化和燕山運動的動力學機制。