Geodetic slip rates in the southern San Andreas Fault system: Effects of elastic heterogeneity and fault geometry-Reference-Cited by-同舟云学术

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Geodetic slip rates in the southern San Andreas Fault system: Effects of elastic heterogeneity and fault geometry

Published:2013-02 Issue:2 Volume:118 Page:689-697
ISSN:2169-9313
Container-title:Journal of Geophysical Research: Solid Earth
language:en
Short-container-title:J. Geophys. Res. Solid Earth

Author:

Lindsey E. O.¹,Fialko Y.¹

Affiliation:

1. Institute of Geophysics and Planetary Physics, Scripps Institution of Oceanography; University of California San Diego; La Jolla California USA

Publisher

American Geophysical Union (AGU)

Subject

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

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1029/2012JB009358/fullpdf

Reference51 articles.

1. Three-dimensional models of elasto-static deformation in heterogeneous media, with applications to the Eastern California Shear Zone;Barbot;Geophys. J. Int.,2009

2. Constraints on fault slip rates of the southern california plate boundary from gps velocity and stress inversions;Becker;Geophys. J. Int.,2005

3. Uncertainties in slip-rate estimates for the Mission Creek strand of the southern San Andreas fault at Biskra Palms Oasis, southern California;Behr;Geol. Soc. Am. Bull.,2010

4. Global positioning system constraints on fault slip rates in southern California and northern Baja, Mexico;Bennett;J. Geophys. Res.,1996

5. Codependent histories of the San Andreas and San Jacinto fault zones from inversion of fault displacement rates;Bennett;Geology,2004

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