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首页> 外文期刊>Geophysical Research Letters >Restoration of interplate locking after the 2005 Off-Miyagi Prefecture earthquake, detected by GPS/acoustic seafloor geodetic observation
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Restoration of interplate locking after the 2005 Off-Miyagi Prefecture earthquake, detected by GPS/acoustic seafloor geodetic observation

机译:GPS /声学海底大地观测发现的2005年宫城县地震后板间锁定的恢复

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摘要

A 7.2-magnitude earthquake occurred on the plate boundary off Miyagi Prefecture, northeastern Japan, on 16 August 2005. From seafloor geodetic observations using the GPS/acoustic combination technique in this area, we have detected notable seafloor movements associated with, and subsequent to this event. The time series of horizontal coordinates obtained at the seafloor reference point MYGW, located about 10 km east of the epicenter, indicates that the strain accumulated for the interseismic period was partly released by the event and a constant strain accumulation restarted after 1-2 years of the post-seismic period with an erratic movement. The horizontal velocity of MYGW after the restart above is estimated to be about 5.7 cm/year toward WNW relative to the Eurasian plate. Our result is consistent with those derived from terrestrial GPS measurements and implies that the interplate locking was restored in the rupture area of the 2005 event around 2007.
机译:2005年8月16日,在日本东北部宫城县板块边界发生了7.2级地震。通过使用GPS /声波组合技术在该地区进行海底大地观测,我们发现了与此有关的海底运动,并在此之后进行了观测。事件。在震中以东约10 km处的海底参考点MYGW上获得的水平坐标的时间序列表明,地震期间部分释放了在地震期间积累的应变,并且在1-2年的地震之后重新开始了恒定的应变积累。后地震时期的动荡不定。相对于欧亚板块,以上重启后,MYGW的水平速度估计为大约5.7厘米/年。我们的结果与从地面GPS测量获得的结果一致,并暗示在2007年前后2005年事件的破裂区域恢复了板间锁定。

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