A possibility of crustal deformation caused by deep fluid flow during long-term slow slip events in the Tokai area.

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ADS bibcode
2019AGUFM.T43H0433U
year
2019
Listed Authors
Umemiya, Y.
Tanaka, Y.
Listed Institutions
Department of Earth and Planetary science, University of Tokyo, Bunkyo-ku, Japan
Department of Earth and Planetary science, University of Tokyo, Bunkyo-ku, Japan

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