Ordering the 2011 Tohoku foreshocks by event number reveals two phases: a linear (constant-rate) phase followed by an exponential phase, with a deactivation coefficient jumping from 0 to 0.065.
Interpretation of the Omori Law
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abstract
The known Omori law is presented in the form of differential equation that describes the evolution of the aftershock activity. This equation is derived hypothetically with taking into account deactivation of the faults in epicentral zone of the main shock. A generalization of the Omori law is proposed.
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Relativity of Time in Earthquake Physics
Ordering the 2011 Tohoku foreshocks by event number reveals two phases: a linear (constant-rate) phase followed by an exponential phase, with a deactivation coefficient jumping from 0 to 0.065.