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  1. 防災科研関係論文

Coseismic and postseismic elastic wave velocity variations caused by the 2008 Iwate-Miyagi Nairiku earthquake, Japan

https://nied-repo.bosai.go.jp/records/4564
https://nied-repo.bosai.go.jp/records/4564
d348fa3f-02e9-4350-a2aa-a245e3283a6a
Item type researchmap(1)
公開日 2023-03-30
タイトル
言語 en
タイトル Coseismic and postseismic elastic wave velocity variations caused by the 2008 Iwate-Miyagi Nairiku earthquake, Japan
言語
言語 eng
著者 M. Hobiger

× M. Hobiger

en M. Hobiger

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U. Wegler

× U. Wegler

en U. Wegler

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K. Shiomi

× K. Shiomi

en K. Shiomi

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H. Nakahara

× H. Nakahara

en H. Nakahara

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抄録
内容記述タイプ Other
内容記述 We analyze coseismic and postseismic velocity variations caused by the June 13, 2008 Iwate-Miyagi Nairiku earthquake (M-W = 6.9) using Passive Image Interferometry (PII). Seismic noise is correlated in order to reconstruct the Green's function between two sensors. Shear wave velocity changes are determined by relating the coda parts of the daily Green's functions to a long-term reference Green's function. Our study extends from January 2008 to August 2010 and includes the correlations for 190 station pairs in three different frequency ranges from 0.125 to 1.0 Hz. We show that combining the 9 different component cross-correlation functions stabilizes the velocity change estimation and increases analysis resolution. The observed velocity change curves can be fitted by model time series consisting of a coseismic velocity drop followed by logarithmic postseismic recovery and seasonal velocity variations. The coseismic velocity drops are stronger at higher frequencies and are concentrated in the southern part of the fault zone. A tomography algorithm was developed to reproject the observed velocity variations of the different sensor pairs onto the single sensors. The depth distribution of coseismic changes was modeled for the three stations with the largest velocity drops. At two stations, the coseismic velocity changes are located in the upper several hundred meters. The third station shows indications for deeper changes, in the order of kilometers. Postseismic recovery takes significantly longer than the analyzed two year period. Seasonal velocity variations with periods of one year are observed at all analyzed frequencies for most station pairs.
言語 en
書誌情報 en : JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH

巻 117, 号 B9, 発行日 2012-09
出版者
言語 en
出版者 AMER GEOPHYSICAL UNION
ISSN
収録物識別子タイプ EISSN
収録物識別子 2169-9356
DOI
関連識別子 10.1029/2012JB009402
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