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2016年日本熊本地震破裂时空过程联合反演

蒋生淼 易磊 张旭 温扬茂

地震学报2018,Vol.40Issue(1):13-23,11.
地震学报2018,Vol.40Issue(1):13-23,11.DOI:10.11939/jass.20170097

2016年日本熊本地震破裂时空过程联合反演

Joint inversion of teleseismic and co-seismic InSAR data for the rupture process of the 2016 Kumamoto earthquake in Japan

蒋生淼 1易磊 2张旭 1温扬茂2

作者信息

  • 1. 中国北京 100081 中国地震局地球物理研究所
  • 2. 中国武汉 430079 武汉大学测绘学院
  • 折叠

摘要

Abstract

On April 15,2016,a disastrous earthquake struck Kumamoto county in Japan.Aiming to further understand the complexity of the earthquake rupture in detail,we conduct a joint inversion of teleseismic waveforms and co-seismic InSAR data for the spatio-temporal rupture process of this earthquake.The results show that,the whole process lasted for about 25 s and released scalar moment up to 6.03 × 1019 N· m,corresponding to moment magnitude MW7.1.The major co-seismic slip distribution was centered in shallow region,and it was dominated by dextral strike.But the rupture had strong normal characteristics in the range of 0-5 km along the dip direction.The maximum co-seismic slip is about 4.9 m,and the major rupture patch was about 5-10 km away from the initial rupture point opposite to the strike direction.In the early stage (0-7 s),it ruptured toward to the shallow region along the dip direction,and ruptured bilaterally along strike direction;about 7 slater,it ruptured to ward to the northeast opposite to the strike direction.The joint inversion results suggest that the Kumamoto earthquake may rupture to the earth surface.

关键词

2016年熊本地震/远场体波/同震InSAR资料/地震破裂过程/联合反演

Key words

2016 Kumamoto earthquake/teleseismic body waveforms/co-seismic InSAR data/earthquake rupture process/joint inversion

分类

天文与地球科学

引用本文复制引用

蒋生淼,易磊,张旭,温扬茂..2016年日本熊本地震破裂时空过程联合反演[J].地震学报,2018,40(1):13-23,11.

基金项目

中央公益类科研院所基本科研业务专项(DQJB16B17)资助. (DQJB16B17)

地震学报

OA北大核心CSCDCSTPCD

0253-3782

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