References

d'Alessio, M. A., Johanson, I. A., Bürgmann, R., Schmidt, D. A. and Murray, M. H., Slicing up the San Francisco Bay Area: Block kinematics and fault slip rates from GPS-derived surface velocities, J. Geophys. Res., 110, B0640, 2007.

Chen, Q. and Freymueller, J. T., Geodetic evidence for a near-fault compiant zone along the San Andreas Fault in the San Francisco Bay Area, J. Geophys. Res., 92, 2002.

Chéry, J., Zoback, M. and Hassani, R., Rheology, strain and stress of the San Andreas Dault in Central and Northern California: A 3-d thermomechanical modeling study, J. Geophys. Res., 106, , B08406, 2001.

Freymueller, J. T., Murray, M. H., Segall, P. and Castillo, D., Kinematics of the Pacific-North America plate boundary zone, northern california, J. Geophys. Res., 104, 7419-7442, 1999.

Funning, G. J., Bürgmann, R., Ferretti, A. and Fumagalli, A. Creep on the rodgers creek fault, northern san francisco bay area from 10 year ps-insar dataset. submitted, 2007.

Le Pichon, X., Kreemer, C. and Chamot-Rooke, N., Asymmetry in elastic properties and the evolution of large continental strike-slip faults, J. Geophys. Res., 110, B03405, 2005.

Lisowski, M., Savage, J. C. and Prescott, W. H., The Velocity Field Along the San Andreas Fault in Central and Southern California, J. Geophys. Res., 96, 8369-8389, 1991.

Prescott, W. H. and Yu, S. B., Geodetic measurement of horizontal deformation in the northern San Francisco Bay region, California, J. Geophys. Res., 91, 7475-7484, 1986

Savage, J. and Burford, R., Geodetic determination of relative plate motion in central California, J. Geophys. Res., 1973

Figure 2.67: A. Best fit dislocation models for the Point Reyes profile. The black dots are the fault-parallel projected GPS velocities with their associated error bars. The grey dots are the PS-SAR data from (Funning et al., 2007). The dashed line is the best classic (elastic half-space) dislocation model. The continuous line is our preferred asymmetric model with a K ratio of $0.41$ that better matches the observed velocity of the westernmost GPS site on the Farallon Islands. B. Trade off between the Locking Depth and the Slip Rate on the SAF. Contoured values are the sum of the weighted squared residuals divided by the number of data points C. Trade off between the Asymmetry Ratio and the Locking Depth on the SAF. D. Trade off between the Asymmetry Ratio and the Slip Rate on the SAF.
\begin{figure*}\begin{center}
\epsfig{file=jolivet07_1_2.eps, width=10cm}\end{center}\end{figure*}

Berkeley Seismological Laboratory
215 McCone Hall, UC Berkeley, Berkeley, CA 94720-4760
Questions or comments? Send e-mail: www@seismo.berkeley.edu
© 2007, The Regents of the University of California