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  1. 防災科研関係論文

Surface wave group velocity in the Osaka sedimentary basin, Japan, estimated using ambient noise cross-correlation functions

https://nied-repo.bosai.go.jp/records/5064
https://nied-repo.bosai.go.jp/records/5064
7d15e716-1a59-4d56-91e4-05629b556848
Item type researchmap(1)
公開日 2023-03-30
タイトル
言語 en
タイトル Surface wave group velocity in the Osaka sedimentary basin, Japan, estimated using ambient noise cross-correlation functions
言語
言語 eng
著者 Kimiyuki Asano

× Kimiyuki Asano

en Kimiyuki Asano

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Tomotaka Iwata

× Tomotaka Iwata

en Tomotaka Iwata

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Haruko Sekiguchi

× Haruko Sekiguchi

en Haruko Sekiguchi

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Kazuhiro Somei

× Kazuhiro Somei

en Kazuhiro Somei

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Ken Miyakoshi

× Ken Miyakoshi

en Ken Miyakoshi

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Shin Aoi

× Shin Aoi

en Shin Aoi

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Takashi Kunugi

× Takashi Kunugi

en Takashi Kunugi

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抄録
内容記述タイプ Other
内容記述 Inter-station cross-correlation functions estimated using continuous ambient noise or microtremor records were used to extract the seismic wave propagation characteristics of the Osaka sedimentary basin, Japan. Temporary continuous observations were conducted at 15 sites in the Osaka basin between 2011 and 2013. The data were analyzed using seismic interferometry. The target period range was 2-8 s. Cross-correlations between all of the possible station pairs were calculated and stacked to produce a year-long data set, and Rayleigh wave signals in the vertical and radial components and Love wave signals in the transverse component were identified from the results. Simulation of interstation Green's functions using the finite difference method was conducted to check the performance of the current three-dimensional velocity structure model. The measured time lag between the observed and theoretical Green's functions was less than 2 s for most station pairs, which is less than the wave period of interest in the target frequency range. Group velocity tomography was applied to group delay times estimated by means of multiple filter analysis. The estimated group velocities for longer periods of 5-8 s exhibited spatial variation within the basin, which is consistent with the bedrock depth distribution; however, the group velocities for shorter periods of 2-3 s were almost constant over the studied area. The waveform and group velocity information obtained by seismic interferometry analysis can be useful for future reconstruction of a three-dimensional velocity structure model in the Osaka basin.
言語 en
書誌情報 en : EARTH PLANETS AND SPACE

巻 69, 号 69
出版者
言語 en
出版者 SPRINGER HEIDELBERG
ISSN
収録物識別子タイプ ISSN
収録物識別子 1880-5981
DOI
関連識別子 10.1186/s40623-017-0694-3
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