Geoelectrical evidence of fluid controlling slow and regular earthquakes along a plate interface

Geoelectrical evidence of fluid controlling slow and regular earthquakes along a plate interface

Abstract Understanding the distribution of physical properties around shallow subducting plate interfaces, where both destructive and “slow” earthquakes occur due to rapid and slower fault slips, respectively, presents a major scientific and disaster mitigation challenge. Pore water is a key factor...

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Bibliographic Details
Main Authors: Hayato Nakamura, Hiroshi Ichihara, Tada-nori Goto, Tetsuo Matsuno, Noriko Tada, Manaka Kuroda, Shinya Sato
Format: Article
Language:English
Published: Nature Portfolio 2025-05-01
Series:Scientific Reports
Subjects:
Plate interface
Seamount
Hyuga-nada
Electrical resistivity
OBEM
Slow earthquakes
Online Access:https://doi.org/10.1038/s41598-025-01440-1
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https://doi.org/10.1038/s41598-025-01440-1

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