Constant dimensionality of fault roughness from the scale of micro-fractures to the scale of continents

Author:

Renard François12,Candela Thibault13,Bouchaud Elisabeth45

Affiliation:

1. ISTerre; University of Grenoble I and CNRS; Grenoble France

2. Physics of Geological Processes; University of Oslo; Oslo Norway

3. Department of Geosciences; Pennsylvania State University; Pennsylvania USA

4. ESPCI, UMR Gulliver/EC2M, 10; Paris Cedex 05 France

5. CEA-Saclay, DSM/IRAMIS/SPEC; Gif-sur-Yvette Cedex France

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Reference33 articles.

1. Mechanics of oblique spreading and ridge segmentation;Abelson;Earth Planet. Sc. Lett.,1997

2. Fractal dimension of fractured surfaces: A universal value?;Bouchaud;Europhys. Lett.,1990

3. Scaling properties of cracks;Bouchaud;J. Phys. C: Condensed Matter,1997

4. Failure of heterogeneous materials: A dynamic phase transition?;Bonamy;Physics Reports,2011

5. Fault smooth gradually as a function of slip;Brodsky;Earth Planet. Sc. Lett.,2011

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