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北海道大学地球物理学研究報告 = Geophysical bulletin of Hokkaido University >
第72号 >

北海道えりも沖における海底地震観測から得られた地震活動

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Please use this identifier to cite or link to this item:http://doi.org/10.14943/gbhu.72.23

Title: 北海道えりも沖における海底地震観測から得られた地震活動
Other Titles: Seismic activities deduced from ocean bottom seismographic observation off Cape Erimo, Hokkaido
Authors: 一條, 和宏1 Browse this author
村井, 芳夫2 Browse this author →KAKEN DB
町田, 祐弥3 Browse this author
三浦, 亮4 Browse this author
西村, 裕一5 Browse this author
高波, 鐡夫6 Browse this author
Authors(alt): Ichijo, Kazuhiro1
Murai, Yoshio2
Machida, Yuya3
Miura, Ryo4
Nishimura, Yuichi5
Takanami, Tetsuo6
Issue Date: 15-Mar-2009
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: 72
Start Page: 23
End Page: 35
Abstract: Observation of micro-earthquakes using Ocean Bottom Seismometers (OBSs) was carried out from May 17 to July 2, 2007 to obtain seismic activities beneath the area off Cape Erimo, Hokkaido. In this neighboring region, large earthquakes with magnitude around 8 occurred at intervals of 40̃60 years. In this study area, clusters of micro-earthquakes were detected immediately before the 2003 Tokachi-oki earthquake (M8.0) by a previous OBS observation (Takanami et al., 2005). The purpose of this study is to investigate the seismic activity after the 2003 Tokachi-oki earthquake by comparing with the results by Takanami et al. (2005). Most of the hypocenters determined in this study are located at shallower depth than those by the Japan Meteorological Agency (JMA). This means that it is difficult to obtain detailed micro-seismicity in offshore area by using land stations only. Therefore, ocean bottom seismographic observations are necessary to detect micro-earthquakes in the region far from the land. According to the depth of the subducting Pacific plate, which is about 10km beneath this study area, it is interpreted that most of these earthquakes occurred at the plate boundary. Seismic activities in this study area were lower than those by Takanami et al. (2005), but some concentrated earthquakes were detected. However, there was no temporal concentration. This suggests that cumulated stress was released by the 2003 Tokachi-oki earthquake and the following post-seismic slip and that the seismicity of this area returns to the steady state.
Type: bulletin (article)
URI: http://hdl.handle.net/2115/38143
Appears in Collections:北海道大学地球物理学研究報告 = Geophysical bulletin of Hokkaido University > 第72号

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