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。
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.
皮质较厚的以及在这区域连接更好的人的转变速率更快。
People whose cortex was thicker and better connected in this region had faster switch rates.
青藏高原区域水平方向形变速率和GPS观测结果吻合较好。
The calculated horizontal velocities are well consistent with GPS surveys.
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