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Hypocenter distribution of the main- and aftershocks of the 2005 Off Miyagi Prefecture earthquake located by ocean bottom seismographic data

机译:利用海底地震资料确定的2005年宫城县地震的主震和余震的震源分布

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摘要

The preliminary hypocenter distribution of the 2005 Off Miyagi Prefecture earthquake and its aftershocks is estimated using data from five ocean bottom and six onshore seismic stations located around the rupture area of the earthquake. The epicenter of the mainshock is relocated at 38.17°N, 142.18°E, and the focal depth is estimated to be 37.5 km. The aftershocks surrounding the mainshock hypocenter form several clusters that are concentrated along a distinct landward dipping plane corresponding to the plate boundary imaged by the previous seismic experiment. The strike and dip angles of the plane agree well with those of the focal mechanism solution of the mainshock. The size of the plane is about 20×25 km2 in the strike and dip directions, which is similar to that of the large coseismic slip area. The up-dip end of the planar distribution of the aftershocks corresponds to the bending point of the subducting oceanic plate, suggesting that the geometry of the plate boundary affects the spatial extent of the asperity of the 2005 earthquake.
机译:使用来自地震破裂区域周围的五个海底和六个陆上地震台站的数据,估算了2005年宫城县外地震及其余震的初步震中分布。主震的震中位于北纬38.17°,东经142.18°,震源深度估计为37.5 km。围绕主震震源的余震形成了几个星团,这些星团沿着与先前地震实验所成像的板块边界相对应的不同的陆上倾角平面集中。飞机的打击角和俯仰角与主震的焦点机制解决方案相吻合。飞机在走向和俯冲方向上的大小约为20×25 km 2 ,与大同震滑移区域的大小相似。余震平面分布的上端对应于俯冲洋板的弯曲点,这表明板边界的几何形状会影响2005年地震的隆起的空间范围。

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