Spatio-temporal changes in the seismic velocity induced by the 2011 Tohoku-Oki earthquake and slow slip event revealed from seismic interferometry, using ocean bottom seismometer’s records

Spatio-temporal changes in the seismic velocity induced by the 2011 Tohoku-Oki earthquake and slow slip event revealed from seismic interferometry, using ocean bottom seismometer’s records

Abstract Seismic interferometry is one of the most effective techniques for detecting temporal variations in seismic velocity caused by large earthquakes. Before the 2011 Tohoku-Oki earthquake (M w 9.0) near the Japan Trench, a slow slip event (SSE, M w 7.0) and low-frequency tremors were observed n...

Full description

Bibliographic Details
Main Authors: Miyuu Uemura, Yoshihiro Ito, Kazuaki Ohta, Ryota Hino, Masanao Shinohara
Format: Article
Language:English
Published: SpringerOpen 2018-12-01
Series:Progress in Earth and Planetary Science
Subjects:
Ambient noise
Autocorrelation function
Seismic interferometry
Slow slip event
Online Access:http://link.springer.com/article/10.1186/s40645-018-0240-3

Internet

http://link.springer.com/article/10.1186/s40645-018-0240-3

Similar Items