Bridging the gap between seismically and geodetically detected slow earthquakes-Reference-Cited by-同舟云学术

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Bridging the gap between seismically and geodetically detected slow earthquakes

Published:2008-05 Issue:10 Volume:35 Page:
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophys. Res. Lett.

Author:

Ide Satoshi¹,Imanishi Kazutoshi²,Yoshida Yasuhiro³,Beroza Gregory C.⁴,Shelly David R.⁵

Affiliation:

1. Department of Earth and Planetary Science; University of Tokyo; Tokyo Japan

2. National Institute of Advanced Industrial Science and Technology; Tsukuba Japan

3. Meteorological Research Institute; Tsukuba Japan

4. Department of Geophysics; Stanford University; Stanford California USA

5. Department of Earth and Planetary Science; University of California; Berkeley California USA

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1029/2008GL034014/fullpdf

Reference21 articles.

1. Vertical seismic noise at very low frequencies;Agnew;J. Geophys. Res.,1978

2. A high-frequency secondary event during the 2004 Parkfield earthquake;Allmann;Science,2007

3. Repeating short- and long-term slow slip events with deep tremor activity around the Bungo channel region, southwest Japan;Hirose;Earth Planets Space,2005

4. Does apparent stress vary with earthquake size?;Ide;Geophys. Res. Lett.,2001

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