Seismic Imaging of a Bimaterial Interface Along the Hayward Fault, CA, with Fault Zone Head Waves and Direct P Arrivals
Author:
Publisher
Springer Science and Business Media LLC
Subject
Geochemistry and Petrology,Geophysics
Link
http://link.springer.com/content/pdf/10.1007/s00024-014-0784-0.pdf
Reference71 articles.
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2. Ampuero, J.-P. and Ben-Zion, Y., 2008, Cracks, pulses and macroscopic asymmetry of dynamic rupture on a bimaterial interface with velocity-weakening friction, Geophys. J. Int., 173, 674–692, doi: 10.1111/j.1365-246X.2008.03736.x .
3. Andrews, D.J., and Ben‐Zion, Y., 1997, Wrinkle‐like slip pulse on a fault between different materials, J. Geophys. Res., 102(B1), 553–571.
4. Bennington, N.L., Thurber, C., Peng, Z., Zhang, H., and Zhao, P., 2013, Incorporating fault zone head wave and direct wave secondary arrival times into seismic tomography: Application at Parkfield, California, J. Geophys. Res., 118, 1008–1014.
5. Ben-Zion, Y., 1989, The response of two joined quarter spaces to SH line sources located at the material discontinuity interface, Geophys. J. Int., 98, 213–222.
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