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Slip distribution of the 2011 off the Pacific coast of Tohoku Earthquake inferred from geodetic data

机译:根据大地测量数据推断的2011年东北太平洋太平洋沿岸滑动分布

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We analyze geodetic observation data associated with the 2011 Tohoku Earthquake to estimate coseismic and early postseismic fault slip distribution on the Pacific plate interface. The maximum slip and the moment magnitude of the main shock are about 60 m and Mw 9.0, respectively. The location of the main slip patch is complementary to the source region of large earthquakes at least for those which have occurred during the last 100 years, and the maximum slip was corresponded to a release of stress accumulation for about 700 years. Source regions of the 1936, 1938, and 1978 earthquakes are considered to have been re-ruptured in the 2011 main shock, where the slip amount was significantly smaller than the main patch.
机译:我们分析了与2011年东北地震有关的大地观测数据,以估计太平洋板块界面上的同震和震后断层滑动分布。主冲击的最大滑移和力矩大小分别约为60 m和Mw 9.0。至少对于最近100年内发生的地震,主滑动斑块的位置与大地震的震源区域互补,并且最大滑动对应于约700年的应力累积释放。 1936、1938和1978年地震的震源区被认为在2011年主震中再次破裂,其滑动量明显小于主震区。

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