Pore Fluid Pressure Development in Compacting Fault Gouge in Theory, Experiments, and Nature

Author:

Faulkner D. R.1ORCID,Sanchez-Roa C.2ORCID,Boulton C.13,den Hartog S. A. M.1

Affiliation:

1. Rock Deformation Laboratory, Department of Earth, Ocean and Ecological Sciences; University of Liverpool; Liverpool UK

2. Departamento de Geología y CEACTierra, Unidad Asociada IACT (CSIC-UGR); Universidad de Jaén; Jaén Spain

3. Now at School of Geography, Environment, and Earth Sciences; Victoria University of Wellington; Wellington New Zealand

Funder

Natural Environment Research Council

Leverhulme Trust

Royal Society

Research Training Grant

Publisher

American Geophysical Union (AGU)

Subject

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

Reference65 articles.

1. Water and argon permeability of phyllosilicate powders under medium to high pressure;Behnsen;Journal of Geophysical Research,2011

2. A note on the oscillating flow method for measuring rock permeability;Bernabe;International Journal of Rock Mechanics and Mining Sciences,2006

3. A thermal pressurization model for the spontaneous dynamic rupture propagation on a three-dimensional fault: 1. Methodological approach;Bizzarri;Journal of Geophysical Research,2006

4. An earthquake mechanism based on rapid sealing of faults;Blanpied;Nature,1992

5. The importance of overpressure timing and permeability evolution in fine-grained sediments undergoing shear;Bolton;Journal of Structural Geology,1998

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