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Tectonic implications of the September 2011 Sikkim earthquake and itsTI Tectonic implications of the September 2011 Sikkim earthquake and its aftershocks

机译:2011年9月锡金地震的构造意义及其TI 2011年9月锡金地震及其余震的构造意义

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This study presents results of the spatial patterns of 292 aftershocks of the Mw 6.9 Sikkim earthquake of September 2011, accurately located through analysis of three component waveforms registered by a five station broadband network operated immediately after its occurrence. Refined hypocentral parameters achieved through application of the hypoDD relocation scheme reveal tight clustering of events along a NW-SE trend with focal depths reaching similar to 60 km. These trends viewed in conjunction with the strike-slip mechanisms of past earthquakes in Sikkim, including the main shock, affirm the predominance of transverse tectonics in this segment of the Himalaya where the Indian plate convergence seems to be accommodated by dextral motion along steeply dipping fault systems.
机译:这项研究提出了2011年9月锡金(Mw 6.9)地震的292次余震的空间格局结果,这些空间格局是通过分析五站宽带网络在发生后立即运行记录的三个分量波形而准确定位的。通过应用hypoDD重定位方案获得的精确的震中参数揭示了沿NW-SE趋势的事件紧密聚集,震源深度达到60 km左右。将这些趋势与锡金过去地震的走滑机制(包括主要地震)一起观察,证实了喜马拉雅山这一段横向构造的优势,那里的印度板块融合似乎是由沿陡倾断层的右旋运动调节的。系统。

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