A possibility of crustal deformation caused by deep fluid flow during long-term slow slip events in the Tokai area.
- 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
Linked Authors [?]
Linked Institutions