Possible shallow slow slip events in Hyuga-nada, Nankai subduction zone, inferred from migration of very low frequency earthquakes-Reference-Cited by-同舟云学术

Possible shallow slow slip events in Hyuga-nada, Nankai subduction zone, inferred from migration of very low frequency earthquakes

Published:2015-01-23 Issue:2 Volume:42 Page:331-338
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophys. Res. Lett.

Author:

Asano Youichi¹,Obara Kazushige²,Matsuzawa Takanori¹,Hirose Hitoshi³,Ito Yoshihiro⁴

Affiliation:

1. National Research Institute for Earth Science and Disaster Prevention; Tsukuba Japan

2. Earthquake Research Institute; University of Tokyo; Tokyo Japan

3. Research Center for Urban Safety and Security; Kobe University; Kobe Japan

4. Disaster Prevention Research Institute; Kyoto University; Kyoto Japan

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1002/2014GL062165/fullpdf

Reference32 articles.

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2. Asano , Y. 2010 Activity of very-low-frequency earthquakes in and around Japan http://cais.gsi.go.jp/YOCHIREN/report/kaihou84/01_02.pdf

3. Spatiotemporal distribution of very-low frequency earthquakes in Tokachi-oki near the junction of the Kuril and Japan trenches revealed by using array signal processing;Asano;Earth Planets Space,2008

4. A discrete episode of seismic and aseismic deformation of the Nankai trough subduction zone accretionary prism and incoming Philippine Sea plate;Davis;Earth Planet. Sci. Lett.,2006

5. Headquarters for Earthquake Research Promotion 2004 Long-term evaluation of occurrence potentials or subduction-zone earthquakes in Hyuga-nada and Ryukyu areas [in Japanese] http://www.jishin.go.jp/main/chousa/04feb_hyuganada/index.html

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