Temporal gravity anomalies observed in the Tokai area and a possible relationship with slow slips

Temporal gravity anomalies observed in the Tokai area and a possible relationship with slow slips

Abstract The water in Earth’s mantle is closely related with plate subduction and volcanism. Recent studies revealed that the mantle wedge corner at approximately 30 km depth holds high-pressure water, where many slow earthquakes occur. To quantify how such water behaves during slow earthquakes help...

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Bibliographic Details
Main Authors: Yoshiyuki Tanaka, Takehito Suzuki, Yuichi Imanishi, Shuhei Okubo, Xinlin Zhang, Miwako Ando, Atsushi Watanabe, Mamoru Saka, Chiaki Kato, Shuichi Oomori, Yoshifumi Hiraoka
Format: Article
Language:English
Published: SpringerOpen 2018-02-01
Series:Earth, Planets and Space
Subjects:
Gravity
Slow earthquakes
Slow slip
Poroelasticity
Water
GNSS
Online Access:http://link.springer.com/article/10.1186/s40623-018-0797-5

Internet

http://link.springer.com/article/10.1186/s40623-018-0797-5

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