Background seismicity in Boso Peninsula, Japan: Long-term acceleration, and relationship with slow slip events

Author:

Reverso T.123,Marsan D.12,Helmstetter A.24,Enescu B.5

Affiliation:

1. ISTerre, Université de Savoie Mont Blanc; Le Bourget-du-Lac France

2. CNRS, ISTerre; Le Bourget-du-Lac France

3. Now at School of Physical Sciences; University of Adelaide; SA Australia

4. ISTerre, Université Grenoble-Alpes; Grenoble France

5. Department of Geophysics, Graduate School of Science; Kyoto University Kitashirakawa; Oiwake-cho, Sakyo-ku, Kyoto Japan

Funder

EC REAKT

MARSITE

JSPS KAKENHI

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Reference41 articles.

1. Generation and propagation of G waves from the Niigata earthquake of June 16, 1964. Part 2. Estimation of earthquake moment, released energy, and stress-strain drop from G wave spectrum;Aki;Bull. Earthquake Res. Inst. Tokyo Univ.,1966

2. Microseismicity but no tremor accompanying slow slip in the Hikurangi subduction zone, New Zealand;Delahaye;Earth Planet. Sci. Lett.,2009

3. A constitutive law for rate of earthquake production and its application to earthquake clustering;Dieterich;J. Geophys. Res.,1994

4. The use of earthquake rate changes as a stressmeter at Kilauea volcano;Dieterich;Nature,2000

5. Uncovering the geodetic signature of silent slip through repeating earthquakes;Frank;Geophys. Res. Lett.,2015

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