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Bulletin of the Seismological Society of America; October 1975; v. 65; no. 5; p. 1073-1095
© 1975 Seismological Society of America
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Theoretical basis of some empirical relations in seismology

HIROO KANAMORI and DON L. ANDERSON

SEISMOLOGICAL LABORATORY DIVISION OF GEOLOGICAL AND PLANETARY SCIENCES CALIFORNIA INSTITUTE OF TECHNOLOGY, PASADENA, CALIFORNIA 91125

Abstract

Empirical relations involving seismic moment Mo, magnitude MS, energy ES and fault dimension L (or area S) are discussed on the basis of an extensive set of earthquake data (MS greater double equals 6) and simple crack and dynamic dislocation models. The relation between log S and log Mo is remarkably linear (slope ~ 2/3) indicating a constant stress drop {Delta}{sigma}; {Delta}{sigma} = 30, 100 and 60 bars are obtained for inter-plate, intra-plate and "average" earthquakes, respectively. Except for very large earthquakes, the relation MS ~ (2/3) log Mo ~ 2 log L is established by the data. This is consistent with the dynamic dislocation model for point dislocation rise times and rupture times of most earthquakes. For very large earthquakes MS ~ (1/3) log Mo ~ log L ~ (1/3) log ES. For very small earthquakes MS ~ log Mo ~ 3 log L ~ log ES. Scaling rules are assumed and justified. This model predicts log ES ~ 1.5 MS ~ 3 log L which is consistent with the Gutenberg-Richter relation. Since the static energy is proportional to FormulaL3, where Formula is the average stress, this relation suggests a constant apparent stress {eta}Formula where {eta} is the efficiency. The earthquake data suggest Formula. These relations lead to log S ~ MS consistent with the empirical relation. This relation together with a simple geometrical argument explains the magnitude-frequency relation log N ~MS.




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