其它构造带的断层形变速率都比较低。
The fault deformation rates of other tectonic zones are relatively low.
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.
山西断陷带的断层形变速率最高，是华北地区最重要的活动块体边界；
The Shanxi graben zone has the largest fault deformation rate showing it is the most important block boundary of North China.
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