首页> 外文期刊>Journal of geophysical research. Solid earth: JGR >Hidden aftershocks of the 2011 M_w 9.0 Tohoku, Japan earthquake imaged with the backprojection method
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Hidden aftershocks of the 2011 M_w 9.0 Tohoku, Japan earthquake imaged with the backprojection method

机译:使用反投影方法拍摄的2011年日本东北部M_w 9.0级地震的隐藏余震

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[1] The first 25 h of the aftershock sequence following the 11 March 2011 M_w 9.0 Tohoku, Japan earthquake is investigated using a backprojection method. In total, 600 aftershocks are imaged during this time period. These aftershocks are distributed over a 500 by 300 km area and include many events in the outer rise. The backprojection events are compared with the Japan Meteorological Agency (JMA) catalogue, which is composed of earthquakes recorded by local seismic networks in Japan. Surprisingly, half of the backprojection events are not found in the JMA catalogue. These events cluster near the Japan Trench and in the outer rise and fill in gaps in the spatial distribution of the early aftershock sequence where large main shock slip is thought to have occurred. These results show that the JMA magnitude of completeness is very high near the trench following the 2011 Tohoku main shock, and earthquakes as large as magnitude 6.8 went undetected by local seismic networks.
机译:[1]使用反投影方法研究了2011年3月11日日本东北地区M_w 9.0地震后的余震序列的前25 h。在此期间,总共拍摄了600次余震。这些余震分布在500 x 300 km的区域,并在外层上升带发生了许多事件。将反投影事件与日本气象厅(JMA)目录进行比较,该目录由日本当地地震网络记录的地震组成。令人惊讶的是,在JMA目录中找不到一半的反投影事件。这些事件聚集在日本海沟附近和外部上升,并填补了余震早期序列的空间分布中的空白,据认为该地震发生了较大的主震滑动。这些结果表明,在2011年东北主震发生后,海沟附近的JMA完整性等级非常高,而当地地震网络未发现6.8级地震。

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