The stabilizing effect of high pore-fluid pressure along subduction megathrust faults: Evidence from friction experiments on accretionary sediments from the Nankai Trough-Reference-Cited by-同舟云学术

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

Published:2021-11 Issue: Volume:574 Page:117161
ISSN:0012-821X
Container-title:Earth and Planetary Science Letters
language:en
Short-container-title:Earth and Planetary Science Letters

Author:

Bedford John D.^ORCID,Faulkner Daniel R.^ORCID,Allen Michael J.^ORCID,Hirose Takehiro

Funder

Natural Environment Research Council

Publisher

Elsevier BV

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Reference75 articles.

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3. Slow slip source characterized by lithological and geometric heterogeneity;Barnes;Sci. Adv.,2020

4. The role of grain size and effective normal stress on localization and the frictional stability of simulated quartz gouge;Bedford;Geophys. Res. Lett.,2021

5. Frictional behavior of large displacement experimental faults;Beeler;J. Geophys. Res.,1996

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