断层平均滑动速率是描述和衡量断层活动强度的一个重要指标。
The fault slip rate is an important parameter of describing and measuring the intensity of fault activity.
本文介绍并完善了作者提出的一种根据历史地震资料估计走滑断裂带地表断层平均滑动速率的方法：“均一滑动法”。
In this paper, a method, the uniform slip method, estimating average slip rate along surface trace of strike slip fault zone by historical earthquake data is offered.
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