Interaction of microseisms with crustal heterogeneity: A case study from the San Jacinto fault zone area

Author:

Hillers G.1,Ben-Zion Y.2,Landès M.3,Campillo M.4

Affiliation:

1. Institut des Sciences de la Terre; Université Joseph Fourier; CNRS Grenoble France

2. Department of Earth Sciences; University of Southern CA; Los Angeles USA

3. Institut de Physique du Globe de Paris; Paris France

4. Institut des Sciences de la Terre; Université Joseph Fourier, CNRS; Grenoble France

Funder

European Research Council

Heisenberg fellowship from the German Research Foundation

National Science Foundation

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference83 articles.

1. Seismic velocity structures in the Southern California plate-boundary environment from doube-difference tomography;Allam;Geophys. J. Int.,2012

2. Ocean wave sources of seismic noise;Ardhuin;J. Geophy. Res.,2011

3. The response of two half spaces to point dislocations at the material interface;Ben-Zion;Geophys. J. Int.,1990

4. Seismic radiation from an SH line source in a laterally heterogeneous planar fault zone;Ben-Zion;Bull. Seismol. Soc. Am.,1990

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