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The stabilizing effect of high pore-fluid pressure along subduction megathrust faults: Evidence from friction experiments on accretionary sediments from the Nankai Trough (2022)

First Author: Bedford J

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/10.31223/x5sp6q

Publication URI: http://dx.doi.org/10.31223/x5sp6q

Type: Preprint