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.
Omori's law: a note on the history of geophysics // Phys
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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.