The stabilizing effect of high pore-fluid pressure along subduction megathrust faults: Evidence from friction experiments on accretionary sediments from the Nankai Trough (2021)
Attributed to:
How do earthquake ruptures propagate through clay-rich fault zones?
funded by
NERC
Abstract
No abstract provided
Bibliographic Information
Digital Object Identifier: http://dx.doi.org/10.1016/j.epsl.2021.117161
Publication URI: http://dx.doi.org/10.1016/j.epsl.2021.117161
Type: Journal Article/Review
Parent Publication: Earth and Planetary Science Letters