Synchronous changes in the seismicity rate and ocean-bottom hydrostatic pressures along the Nankai trough: A possible slow slip event detected by the Dense Oceanfloor Network system for Earthquakes and Tsunamis (DONET)
详细信息 查看全文
- 作者：Kensuke Suzukia ; kensukes@jamstec.go.jp" class="auth_mail" title="E-mail the corresponding author ; Masaru Nakanoa ; Narumi Takahashia ; Takane Horia ; Shinichiro Kamiyaa ; Eiichiro Arakia ; Ryoko Nakataa ; Yoshiyuki Kanedaa ; b
- 关键词：DONET ; Seismicity rate changes ; ETAS model ; Ocean-bottom pressure changes ; Slow slip event
- 刊名：Tectonophysics
- 出版年：2016
- 出版时间：12 June 2016
- 年：2016
- 卷：680
- 期：Complete
- 页码：90-98
- 全文大小：1630 K
文摘
- •
We detected the seismicity change off the Kii Peninsula by using DONET data.
- •
We detected the vertical deformation of the seafloor by using the pressure gages.
- •
The seismicity change synchronized with the crustal deformation.
- •
Both changes might be caused by the regional stress change.