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北海道大学地球物理学研究報告 = Geophysical bulletin of Hokkaido University >
第73号 >

高密度観測網のデータを使ったスラブ内地震による強震動の解析 : 島弧の構造との関連

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Please use this identifier to cite or link to this item:http://doi.org/10.14943/gbhu.73.57

Title: 高密度観測網のデータを使ったスラブ内地震による強震動の解析 : 島弧の構造との関連
Other Titles: Analyses of Strong Ground Motions from Intraslab Earthquakes Using High-Density Observation Network Data : Relation to the Island Arc Structure
Authors: 筧, 楽麿1 Browse this author
西條, 裕介2 Browse this author
染井, 一寛3 Browse this author
Authors(alt): KAKEHI, Yasumaro1
SAIJO, Yusuke2
SOMEI, Kazuhiro3
Issue Date: 19-Mar-2010
Publisher: 北海道大学大学院理学研究院自然史科学部門(地球物理学)
Journal Title: 北海道大学地球物理学研究報告
Journal Title(alt): Geophysical bulletin of Hokkaido University
Volume: 73
Start Page: 57
End Page: 70
Abstract: Observed waveforms recorded by the high-density strong ground motion observation network from two intraslab earthquakes are analyzed in detail. One is the 2001 Iwate-ken Nairiku Nanbu earthquake(MJMA = 6.4, depth = 121.5 km), which occurred in the Pacific slab subducting beneath the Tohoku island arc. The other is the 2006 Oita-ken Seibu earthquake(MJMA = 6.2, depth= 145.2 km), which occurred in the Philippine Sea slab subducting beneath the Kyushu island arc. In both cases, observed strong ground motions show singular spatial distribution, where high-frequency seismic waves at the stations located in backarc side of the volcanic front have much smaller amplitudes compared with those at the forearc side stations. This singular distribution of strong ground motions can be interpreted by considering attenuation of high-frequency seismic waves at the backarc side stations due to the wave propagation through the low-Q value zone beneath the volcanic front. In the case of the 2006 Oita-ken Seibu earthquake, effect of high-frequency seismic waves trapped in the high-Q slab is also important. It may cause the large amplitude of high-frequency waves observed at the stations in Chugoku and Shikoku, the shallower-slab side extent of forearc side.
Type: bulletin (article)
URI: http://hdl.handle.net/2115/44457
Appears in Collections:北海道大学地球物理学研究報告 = Geophysical bulletin of Hokkaido University > 第73号

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