Annu. Rev. Earth Planet. Sci. 2005. 33:335–67 doi: 10.1146/annurev.earth.33.092203.122505 Copyright c 2005 by Annual Reviews. All rights reserved First published online as a Review in Advance on January 21, 2005 EARTHQUAKE TRIGGERING BY STATIC,DYNAMIC, AND POSTSEISMIC STRESS TRANSFER Andrew M. Freed Department of Earth and Atmospheric Sciences, Purdue University, West Lafayette, Indiana 47907; email:
[email protected] KeyWords Coulomb, aftershocks, earthquake-clusters, stress-shadows, viscoelastic ■ Abstract Earthquake triggering is the process by which stress changes associ- ated with an earthquake can induce or retard seismic activity in the surrounding region or trigger other earthquakes at great distances. Calculations of static Coulomb stress changes associated with earthquake slip have proven to be a powerful tool in explaining many seismic observations, including aftershock distributions, earthquake sequences, and the quiescence of broad, normally active regions following large earthquakes. De- layed earthquake triggering, which can range from seconds to decades, can be explained by a variety of time-dependent stress transfer mechanisms, such as viscous relaxation, poroelastic rebound, or afterslip, or by reductions in fault friction, such as predicted by rate and state constitutive relations. Rapid remote triggering of earthquakes at great distances (from several fault lengths to 1000s of km) is best explained by the passage of transient (dynamic) seismic waves, which either immediately induce Coulomb-type failure or initiate a secondary mechanism that induces delayed triggering. The pas- sage of seismic waves may also play a significant role in the triggering of near-field earthquakes. INTRODUCTION by PURDUE UNIVERSITY LIBRARY on 04/14/05.