Resolving the discrepancy between geodetic and seismic fault models for the 1989 Loma Prieta, California, earthquake

[1]  W. D. Stuart,et al.  Material heterogeneity simplifies the picture: Loma prieta , 1992, Bulletin of the Seismological Society of America.

[2]  P. Segall,et al.  A fault model for the 1989 Kilauea South Flank Earthquake from leveling and seismic data , 1991 .

[3]  W. Thatcher,et al.  Faulting geometry and slip from co-seismic elevation changes: The 18 October 1989, Loma Prieta, California, earthquake , 1991 .

[4]  Gregory C. Beroza,et al.  Near-source modeling of the Loma Prieta earthquake: Evidence for heterogeneous slip and implications for earthquake hazard , 1991 .

[5]  Jamison H. Steidl,et al.  Rupture history of the 1989 Loma Prieta, California, earthquake , 1991, Bulletin of the Seismological Society of America.

[6]  William L. Ellsworth,et al.  The October 17, 1989, Loma Prieta, California, Earthquake and its aftershocks: Geometry of the sequence from high-resolution locations , 1990 .

[7]  J. C. Savage,et al.  Geodetic estimate of coseismic slip during the 1989 Loma Prieta, California, Earthquake , 1990 .

[8]  J. Sauber,et al.  Geodetic measurement of deformation in the Loma Prieta, California Earthquake with very long baseline interferometry , 1990 .

[9]  Y. Okada.  Surface deformation due to shear and tensile faults in a half-space , 1985 .

[10]  Thomas H. Heaton,et al.  Rupture model of the 1989 Loma Prieta earthquake from the inversion of strong-motion and broadband teleseismic data , 1991, Bulletin of the Seismological Society of America.