首页> 外文期刊>Journal of geophysical research. Solid earth: JGR >Investigation of earthquake jump distance for strike-slip step overs based on 3-D dynamic rupture simulations in an elastic half-space
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Investigation of earthquake jump distance for strike-slip step overs based on 3-D dynamic rupture simulations in an elastic half-space

机译:基于弹性半空间中3-D动态破裂模拟的走滑阶跃地震跳跃距离研究

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摘要

We systematically investigate the distance that dynamically propagating earthquake ruptures could jump across step overs in strike-slip faults set in a homogeneous half-space. The following factors are found to have major effects on the critical jump distance: the dimensionless effective shear stress, the initial normal stress, the Earth's free surface, and the accelerating length of the rupture front on the main fault prior to a jump. An important finding in this study is that the critical jump distance for extensional step overs could exceed 10km under certain conditions, while ruptures on compressional step overs under the same conditions could only jump 6km fault step overs. This may provide a physical explanation for some geological observations of over 10km jump distance in natural earthquake. The critical jump distance usually increases as the dimensionless effective shear stress increases. Without the free surface effect, the critical jump distance for step overs could only reach up to 6km, which is very close to the 5km given by the classic 2-D simulations.
机译:我们系统地研究了在同质半空间中设置的走滑断层中,动态传播的地震破裂可能跨越阶跃而跳变的距离。已发现以下因素对临界跳变距离有重要影响:无因次有效剪切应力,初始法向应力,地球的自由表面以及在跳变之前主要断层上破裂前沿的加速长度。这项研究的重要发现是,在某些条件下,伸展式跨步的临界跳越距离可能超过10km,而在相同条件下,压缩式跨步的破裂只能跳越6km的断层跨步。这可以为自然地震中跳跃距离超过10 km的某些地质观测提供物理解释。临界跳跃距离通常随无因次有效剪切应力的增加而增加。如果没有自由表面效应,则跨步的临界跳跃距离只能达到6km,这非常接近经典2D模拟给出的5km。

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