首页> 外文期刊>Geophysical Research Letters >Mechanical behavior of western alpine structures inferred from statistical analysis of seismicity - art. no. 1224
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Mechanical behavior of western alpine structures inferred from statistical analysis of seismicity - art. no. 1224

机译:从地震活动的统计分析推论出西部高山结构的力学行为。没有。 1224

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1] Two seismic arcs (150 km and 120 km long) located in the western Alps, 50 km apart from each other, are characterized by different statistical patterns in energy and space domains. For the two arcs, we found power-law distributions in energy domain with a lower b-value and fall-off for large events for the easternmost arc only, and roughly similar spatial damage. By comparing the shape and the statistical parameters of these distributions with those provided by numerical models of rock damage, we suggest a relatively more brittle behavior for one area with respect to the other. We discuss the implications of the observed distributions in terms of tectonics and of mechanics of faulting. We suggest three candidates to drive the relative changes in seismicity distribution between the two arcs: the earthquake depth, the host rock composition, and the inherited fracturing patterns. [References: 38
机译:1]位于阿尔卑斯山西部的两个地震弧(分别长150 km和120 km)彼此相距50 km,其能量和空间域的统计模式不同。对于这两个弧线,我们发现能量域中的幂律分布具有较低的b值,并且仅对于最东端的弧线具有较大事件发生衰减,并且空间损害大致相似。通过将这些分布的形状和统计参数与岩石破坏的数值模型提供的形状和统计参数进行比较,我们建议一个区域相对于另一个区域具有相对较脆的行为。我们从构造学和断层力学方面讨论了观测分布的含义。我们建议使用三个候选来驱动两个弧线之间地震分布的相对变化:地震深度,主体岩石成分和继承的压裂模式。 [参考:38

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