Strain rate and temperature dependence of Omori law scaling constants of AE data: Implications for earthquake foreshock-aftershock sequences
Author:
Publisher
American Geophysical Union (AGU)
Subject
General Earth and Planetary Sciences,Geophysics
Reference24 articles.
1. Maximum likelihood estimate of b in the formula log N = a − bm and its confidence limits;Aki;Bull. Earthquake Res. Inst. Univ. Tokyo,1965
2. Time-dependent deformation and failure;Costin,1987
3. Teleseismic b values; or, much Ado about 1.0;Frohlich;J. Geophys. Res.,1993
4. Mainshocks are aftershocks of conditional foreshocks: How do foreshock statistical properties emerge from aftershock laws?;Helmstetter;J. Geophys. Res.,2003
5. Omori's power law aftershock sequences of microfracturing in rock fracture experiment;Hirata;J. Geophys. Res.,1987
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