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Critical Jump Distance for Propagating Earthquake Ruptures Across Step-Overs

机译:跨步传播地震破裂的临界跳变距离

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The geometry of a strike-slip fault system is an important component that influences the kinematics and interactions of the various faults within the system. Discontinuities and bends in the fault geometry not only determine the types of structures and the physiography that we observe along the fault system but also have a significant influence on the propagation of earthquake ruptures. A precise knowledge of the fault geometry, especially how it is segmented and other physical parameters, is essential for seismic hazard analysis. It is known that earthquake ruptures sometimes propagate over multiple faults by jumping from one segment to the next. A fault jump is a sudden dynamic coalescence of two faults separated by a step-over. Field observations suggest that a step-over width of 5 km is an appropriate maximum jump distance. Our study shows that between 2.5 and 6.5 km of step-over width, the probability of fault jump, for both releasing and restraining step-overs, decreases significantly from 100 to < 10 %.
机译:走滑断层系统的几何形状是影响系统内各种断层的运动学和相互作用的重要组成部分。断层几何形状的不连续性和弯曲度不仅决定了我们沿断层系统观察到的构造类型和地貌,而且对地震破裂的传播也有重要影响。准确了解断层几何形状,尤其是如何对其进行分段以及其他物理参数,对于地震危险性分析至关重要。众所周知,地震破裂有时会通过从一个分段跳到下一个分段而在多个断层上传播。故障跳跃是两个故障之间的突然动态合并,这些故障被一个跨步分开。现场观察表明,5 km的跨步宽度是适当的最大跳跃距离。我们的研究表明,在跨步宽度2.5至6.5 km之间,对于释放和抑制跨步,断层跳跃的可能性从100%显着降低到<10%。

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