crustal horizontal deformation

基本解释

In this paper the model of horizontal crustal deformation with the fitting method is studied and related formulas are derived.
利用这一曲面拟合理论成功地研究了地壳水平形变模型。详细推导了相应的公式。
The modelling results show that the collision of the India Plate with the Eurasia Plate is the main driving force causing crustal horizontal deformation of China.
模拟结果显示：印度板块与欧亚板块的碰撞、挤压是构成中国大陆内部岩石层水平形变的主要驱动力。
Based on the results observed at GPS tracing stations, more accurate movement rate of intraplate and plate margin horizontal crustal deformation in East Asia has been obtained for the first time.
利用GPS跟踪站的观测结果，首次获得了东亚地区板内及板缘地壳水平运动较准确的运动速率，据此分析了我国大陆及周围地区地壳水平运动的特征。