According to above results, the horizontal displacement and strain field caused by the main fault movement have simulated and showed the interactions among boundary faults.
依据上述反演结果，模拟了区域主要断层运动引起的水平位移、应变速率场图像，显示了边界断裂及其之间的相互作用。
It seems that the recent tectonic and earthquake activities gradually move towards the south reaching the great fault of the main boundary.
现在构造活动与地震活动似均逐渐向南移到主边界大断层一带。
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