Stabilization of fault slip by fluid injection in the laboratory and in situ

Author:

Cappa Frédéric12ORCID,Scuderi Marco Maria3ORCID,Collettini Cristiano34ORCID,Guglielmi Yves5ORCID,Avouac Jean-Philippe6

Affiliation:

1. Université Côte d’Azur, CNRS, Observatoire de la Côte d’Azur, IRD, Géoazur, 06560 Sophia Antipolis, France.

2. Institut Universitaire de France, Paris, France.

3. Dipartimento di Scienze della Terra, La Sapienza Università di Roma, Piazzale Aldo Moro 5, 00185 Rome, Italy.

4. Istituto Nazionale di Geofisica e Vulcanologia, via di Vigna Murata 605, 00143 Rome, Italy.

5. Earth and Environmental Sciences, Lawrence Berkeley National Laboratory, Berkeley, CA 94720, USA.

6. Seismological Laboratory, California Institute of Technology, Pasadena, CA 91125, USA.

Abstract

Fluid injection experiments on laboratory and natural faults reveal a similar phase of fault opening and accelerating creep.

Funder

European Research Council

Agence Nationale de la Recherche

Institut Universitaire de France

Marie Sklodowska-Curie grant

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

Reference51 articles.

1. LABORATORY-DERIVED FRICTION LAWS AND THEIR APPLICATION TO SEISMIC FAULTING

2. N. Lapusta S. Barbot Models of earthquakes and aseismic slip based on laboratory-derived rate and state friction laws in The Mechanics of Faulting: From Laboratory to Real Earthquakes A. Bizzarri H. S. Bhat Eds. (Research Signpost 2012) pp. 153–207.

3. Modeling injection-induced seismicity with the physics-based earthquake simulator RSQSim;Dieterich J. H.;Seismol. Res. Lett.,2015

4. Dilatancy, compaction, and slip instability of a fluid-infiltrated fault;Segall P.;J. Geophys. Res.,1995

5. Three-dimensional earthquake sequence simulations with evolving temperature and pore pressure due to shear heating: Effect of heterogeneous hydraulic diffusivity;Noda H.;J. Geophys. Res.,2010

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