High Pore Fluid Pressure May Cause Silent Slip in the Nankai Trough
Shuichi Kodaira(Japan Agency for Marine-Earth Science and Technology), Yoshiyuki Kaneda(Kagawa University), Takashi Iidaka(Earthquake Engineering Research Institute), Takaya Iwasaki(Japan Agency for Marine-Earth Science and Technology), Aitaro Kato(Association for the Development of Earthquake Prediction), Jin‐Oh Park(Japan Agency for Marine-Earth Science and Technology)
Cited by 502
Related Papers
Propagation of Slow Slip Leading Up to the 2011 <i>M</i> <sub>w</sub> 9.0 Tohoku-Oki Earthquake
|Science|2012|792
Connecting slow earthquakes to huge earthquakes
|Science|2016|776
Variations of fluid pressure within the subducting oceanic crust and slow earthquakes
|Geophysical Research Letters|2010|199
A normal-faulting seismic sequence triggered by the 2011 off the Pacific coast of Tohoku Earthquake: Wholesale stress regime changes in the upper plate
|Earth Planets and Space|2011|179
The generation of large earthquakes
|Nature Reviews Earth & Environment|2020|177