Global Omori law decay of triggered earthquakes: Large aftershocks outside the classical aftershock zone

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EARTHQUAKE TRIGGERING BY STATIC, DYNAMIC, AND POSTSEISMIC STRESS TRANSFER (2005, methodology): “In a broad study of earthquake triggering using a global earthquake catalog, Parsons (2002) calculated shear stress changes induced by earthquakes with Ms ≥ 7 on subsequent rupture planes near enough to be potentially triggered.”
Postseismic relaxation driven by brittle creep: A possible mechanism to reconcile geodetic measurements and the decay rate of aftershocks, application to the Chi-Chi earthquake, Taiwan (2004, result): “For comparison, we may also mention that [Parsons, 2002] analysis of triggered events globally obey an Omori law with a characteristic decay time typically between 7 and 11 years.”
Introduction to special section: Stress transfer, earthquake triggering, and time‐dependent seismic hazard (2005, unknown): “Stress triggering of large earthquakes has also been inferred from studies of global catalogs [Parsons, 2002b; Wan et al., 2004; McKernon and Main, 2005] and has been interpreted in terms of ‘‘anomalous’’ or intermittent diffusion in contrast to the homogeneous (or nonintermittent) diffusion…”