The fault slip rate is an important parameter of describing and measuring the intensity of fault activity.
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。
In a presentation to the 18th Caribbean Geological Conference in 2008, the team pointed out that their models showed a slip rate of around 8 millimetres per year on the fault.
在2008年举行的第十八届加勒比海地质学会议上，该小组在报告中指出他们的模型显示这一断层以每年大约8英里的滑行速度移动。
The pattern of the progressive evolution of offset streams might indicate that the slip rate of the fault in the same place is relatively constant during a certain period.
断错水系的演化图象则进一步提供了在一定时段内，同一地点滑动速率基本稳定的线索。
Slip rate, net slip and the Numbers of unstable events depend on the orientation of the fault with respect to the principal stress axes.
每条断层的位移速率、总位移量以及失稳事件数与断层方向和主压应力轴的夹角有关。
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.
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.
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”。
应用推荐