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Title: 諏訪之瀬島火山における火口に近接した地震計アレイ観測 -2010年10月~11月実施-
Other Titles: Seismic Array Observation Close to the Active Crater at Suwanose-jima Volcano, Southwest Japan for the Period from October to November 2010
Authors: 中道, 治久  kyouindb  KAKEN_id  orcid https://orcid.org/0000-0002-5501-0965 (unconfirmed)
青山, 裕  KAKEN_name
西村, 太志  KAKEN_name
八木原, 寛  KAKEN_name
太田, 雄策  KAKEN_name
横尾, 亮彦  KAKEN_name
井口, 正人  kyouindb  KAKEN_id
Author's alias: NAKAMICHI, Haruhisa
AOYAMA, Hiroshi
NISHIMURA, Takeshi
YAKIWARA, Hiroshi
OHTA, Yusaku
YOKOO, Akihiko
IGUCHI, Masato
Keywords: 諏訪之瀬島
地震計アレイ
爆発地震
火山性微動
Suwanose-jima
seismic array
explosion earthquake
volcanic tremor
Issue Date: Sep-2013
Publisher: 京都大学防災研究所
Journal title: 京都大学防災研究所年報. B = Disaster Prevention Research Institute Annuals. B
Volume: 56
Issue: B
Start page: 227
End page: 235
Abstract: We conducted a small-aperture seismic array observation at Suwanose-jima volcano for the period from 1 October to 18 November 2010. The seismic array consists of 13 elements of short-period seismometers and 5 data loggers. We perform array analysis for continuous seismic records observed during this period to investigate the wave-field properties of several episodes of volcanic tremors and 30 explosion earthquakes. Averages of the slowness values and back azimuths of volcanic tremors are estimated to be 0.8-1.4 s/km and 0°-40°, respectively. This suggests that the tremor wave consists of body and surface waves that propagate from the active crater. The array analyses and particle motions of explosion earthquakes indicate that the initial parts of the waveforms of explosion earthquakes are S waves that come from the direction of the active crater. The slowness values of the S waves of the explosion earthquakes are 0.3-0.5 s/km. Variation of the slowness value reflects the depth change of the explosion sources.
URL: http://www.dpri.kyoto-u.ac.jp/nenpo/nenpo.html
URI: http://hdl.handle.net/2433/181544
Appears in Collections:Vol.56 B

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