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首页> 外文期刊>Earth, planets and space: EPS >Coseismic slip distribution of the 2005 off Miyagi earthquake (M7.2) estimated by inversion of teleseismic and regional seismograms
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Coseismic slip distribution of the 2005 off Miyagi earthquake (M7.2) estimated by inversion of teleseismic and regional seismograms

机译:通过远震和区域地震图的反演估计2005年宫城地震(M7.2)的同震滑动分布

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摘要

A large earthquake (M7.2) occurred along the plate boundary off Miyagi Prefecture (Miyagi-Oki), northeastern Japan, on August 16, 2005. In this area, large earthquakes (similar to M7.5) have occurred repeatedly at intervals of about 37 years, and more than 27 years have passed since the last event occurred. To estimate the relationship between this earthquake and the previous events, we determined coseismic slip distribution by this 2005 Miyagi-Oki earthquake by adopting the seismic waveform inversion method of Yagi et al. (2004) and compared it with that of the previous 1978 Miyagi-Oki earthquake. We performed two cases of the inversions; inversion using only far-field seismograms and that using far-field seismograms and local seismograms simultaneously. Both results show that a large slip occurred near the hypocenter and rupture extended to the westward deeper portion. Considering that the rupture area of the 2005 event partly overlapped with the southeastern part of that of the 1978 event, suggests this result the possibility that plural asperities exist which cause the sequence of Miyagi-Oki earthquakes and that the 2005 event ruptured one of such asperities, although the previous 1978 event ruptured all the asperities at one time.
机译:2005年8月16日,在日本东北部宫城县(Miyagi-Oki)的板块边界发生了大地震(M7.2)。在该地区,以自上一次事件发生以来,已经过去了约37年,已经过去了27年。为了估算该地震与先前地震之间的关系,我们采用Yagi等人的地震波形反演方法,确定了这次2005年宫城-大木地震的同震滑动分布。 (2004年),并将其与1978年以前的宫城-冲木地震比较。我们进行了两种情况的反演。仅使用远场地震图进行反演,同时使用远场地震图和局部地震图进行反演。两项结果均表明,在震源附近发生了大的滑移,并且破裂向西扩展。考虑到2005年地震的破裂区域与1978年地震的东南部分重叠,这表明存在可能导致宫城-大木地震序列的多重凹凸不平,而2005年地震破裂了其中一种这样的可能性。 ,尽管上一次1978年的事件一次破灭了所有惨案。

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