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)-Reference-Cited by-同舟云学术

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)

Published:2016-06 Issue: Volume:680 Page:90-98
ISSN:0040-1951
Container-title:Tectonophysics
language:en
Short-container-title:Tectonophysics

Author:

Suzuki Kensuke^ORCID,Nakano Masaru,Takahashi Narumi,Hori Takane,Kamiya Shinichiro,Araki Eiichiro,Nakata Ryoko,Kaneda Yoshiyuki

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geophysics

Reference46 articles.

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2. The detectability of shallow slow earthquakes by the Dense Oceanfloor Network system for Earthquakes and Tsunamis (DONET) in Tonankai district, Japan;Ariyoshi;Mar. Geophys. Res.,2014

3. Offshore geodetic data conducive to the estimation of the afterslip distribution following the 2003 Tokachi-oki earthquake;Baba;Earth Planet. Sci. Lett.,2006

4. Continuous long-term seafloor pressure observation for detecting slow-slip interplate events in Miyagi-Oki on the landward Japan trench slope;Hino;J. Disaster Res.,2009

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