Laboratory observations of time‐dependent frictional strengthening and stress relaxation in natural and synthetic fault gouges-Reference-Cited by-同舟云学术

Laboratory observations of time‐dependent frictional strengthening and stress relaxation in natural and synthetic fault gouges

Published:2016-02 Issue:2 Volume:121 Page:1183-1201
ISSN:2169-9313
Container-title:Journal of Geophysical Research: Solid Earth
language:en
Short-container-title:J. Geophys. Res. Solid Earth

Author:

Carpenter B. M.¹²,Ikari M. J.²³,Marone C.²

Affiliation:

1. School of Geology and Geophysics University of Oklahoma Norman Oklahoma USA

2. Department of Geosciences and Energy Institute Center for Geomechanics, Geofluids, and Geohazards Pennsylvania State University University Park Pennsylvania USA

3. MARUM, Center for Marine and Environmental Science University of Bremen Bremen Germany

Funder

NSF

Publisher

American Geophysical Union (AGU)

Subject

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

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1002/2015JB012136

Reference142 articles.

1. Barchi M. R. G.Lena W.Alvarez F.Felici andA.Lupattelli(2012) Mesoscopic S‐C fabrics in shallow fault zones: A case history from the Umbria‐Marche Apennines (Central Italy)Geophys.Res.Abstracts 14 EGU2012‐10979.

2. 13. Laboratory-Observed Faulting in Intrinsically and Apparently Weak Materials

3. The roles of time and displacement in velocity-dependent volumetric strain of fault zones

4. The roles of time and displacement in the evolution effect in rock friction

5. Earthquake stress drop and laboratory-inferred interseismic strength recovery

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