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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。
Euler vector method was used to establish the intraplate motion model. According to the motion model, we apply the 2-period observation results of the national GPS crustal movement monitoring network to calculate the current amount of movement of the block in China’s mainland. Comparing the GPS results with the geological results of intraplate motion, the comparability of the two reflects the overall movement trend of intraplate in China under the influence of global plate motion.