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Results: 1-7 |
Results: 7
The failure of earthquake failure models
Authors: Gomberg, J
Citation: J. Gomberg, The failure of earthquake failure models, J GEO R-SOL, 106(B8), 2001, pp. 16253-16263
Earthquake triggering by seismic waves following the Landers and Hector Mine earthquakes
Authors: Gomberg, J Reasenberg, PA Bodin, P Harris, RA
Citation: J. Gomberg et al., Earthquake triggering by seismic waves following the Landers and Hector Mine earthquakes, NATURE, 411(6836), 2001, pp. 462-466
On rate-state and Coulomb failure models
Authors: Gomberg, J Beeler, N Blanpied, M
Citation: J. Gomberg et al., On rate-state and Coulomb failure models, J GEO R-SOL, 105(B4), 2000, pp. 7857-7871
Triggering of earthquake aftershocks by dynamic stresses
Authors: Kilb, D Gomberg, J Bodin, P
Citation: D. Kilb et al., Triggering of earthquake aftershocks by dynamic stresses, NATURE, 408(6812), 2000, pp. 570-574
The initial subevent of the 1994 Northridge, California, earthquake: Is earthquake size predictable?
Authors: Kilb, D Gomberg, J
Citation: D. Kilb et J. Gomberg, The initial subevent of the 1994 Northridge, California, earthquake: Is earthquake size predictable?, J SEISMOL, 3(4), 1999, pp. 409-420
Possible cause for an improbable earthquake: The 1997 M-w 4.9 southern Alabama earthquake and hydrocarbon recovery
Authors: Gomberg, J Wolf, L
Citation: J. Gomberg et L. Wolf, Possible cause for an improbable earthquake: The 1997 M-w 4.9 southern Alabama earthquake and hydrocarbon recovery, GEOLOGY, 27(4), 1999, pp. 367-370
The strain in the array is mainly in the plane (Waves below similar to 1 Hz)
Authors: Gomberg, J Pavlis, G Bodin, P
Citation: J. Gomberg et al., The strain in the array is mainly in the plane (Waves below similar to 1 Hz), B SEIS S AM, 89(6), 1999, pp. 1428-1438
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