摘要
应用欧拉矢量方法，建立了板内块体运动模型。根据运动模型，应用全国ＧＰＳ地壳运动监测网２期观测结果，计算了我国大陆板内块体的现今运动量。ＧＰＳ计算结果与板内块体运动的地质结果比较，二者的可比性反映了我国大陆板内块体在全球板块运动影响下的总体运动趋势。
A kinematic model for intraplate rigid blocks is formed by using the Eulerian vector,by which the current motion of continental intraplate blocks of China is computed based on the GPS measurements for two periods in China.Comparing the computational results with the geologic activity of intraplate blocks,the consistence between which indicates the integral motion trend of China continental intraplate blocks under the influence of global plate motion.
出处
《地壳形变与地震》
CSCD
1998年第1期8-13,共6页
Crustal Deformation and Earthquake
基金
国家自然科学基金
国家攀登计划
