EARTHQUAKE TRIGGERING BY STATIC, DYNAMIC, AND POSTSEISMIC STRESS TRANSFER

By A. Freed. 2005

826 citations recorded by the source corpus.

Subfields: Geophysics

View Paper: https://www.semanticscholar.org/paper/03f8c39c227394f9b9220959e84d706518f7571e

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In Geophysics

1. A. Freed
2. N. V. Elst
3. E. Brodsky
4. Roland Bürgmann
5. David P. Hill
6. Zhigang Peng
7. D. Shelly
8. S. Toda

Citations in the corpus

• Triggered creep as a possible mechanism for delayed dynamic triggering of tremor and earthquakes (2011, background): “The triggered fault slip is detectable in the form of earthquake”
• Implications of deformation following the 2002 Denali, Alaska, earthquake for postseismic relaxation processes and lithospheric rheology (2006, background): “Earthquakes do not simply release built-up stress, they redistribute it, a process that greatly influences regional seismicity, sometimes inducing earthquake sequences, other times ushering in periods of seismic quiescence (see reviews by Stein [1999, 2003], King and Cocco [2001], and Freed [2005] ”
• Connecting near-field and far-field earthquake triggering to dynamic strain (2010, background): “The types of stresses that have been proposed as the agents by which one fault transmits a triggering signal to another include coseismic static strain changes, progressive postseismic strain changes (including afterslip and viscous creep), and dynamic strains from radiated seismic waves [ Freed, 20”
• The geophysics, geology and mechanics of slow fault slip (2018, background): “Together with other postseismic relaxation mechanisms, slow slip of either type can enhance static stress changes at large distances from a mainshock and trigger subsequent events (e.g., Hearn et al., 2002, Freed, 2005).”
• Forecasting the evolution of seismicity in southern California : Animations built on earthquake stress transfer : Stress transfer, earthquake triggering, and time-dependent seismic hazard (2005, background): “There is growing evidence that large earthquakes can inhibit or promote failure on nearby faults for decades to centuries, and that the transfer of stress plays a governing role in this interaction [Harris, 1998; Stein, 1999; King and Cocco, 2000; Freed, 2005].”