eprintid: 1475 rev_number: 12 eprint_status: archive userid: 2 dir: disk0/00/00/14/75 datestamp: 2015-02-25 09:09:05 lastmod: 2017-02-08 12:21:40 status_changed: 2015-04-27 12:10:58 type: article metadata_visibility: show creators_name: Parsons, Tom corp_creators: U.S. Geological Survey, Menlo Park, California, USA title: Global Omori law decay of triggered earthquakes: Large aftershocks outside the classical aftershock zone ispublished: pub subjects: SS divisions: EPOS-P full_text_status: none abstract: Triggered earthquakes can be large, damaging, and lethal as evidenced by the1999 shocks in Turkey and the 2001 earthquakes in El Salvador. In this study, earthquakes with Ms ≥ 7.0 from the Harvard centroid moment tensor (CMT) catalog are modeled as dislocations to calculate shear stress changes on subsequent earthquake rupture planes near enough to be affected. About 61% of earthquakes that occurred near (defined as having shear stress change ∣Δτ∣ ≥ 0.01 MPa) the Ms ≥ 7.0 shocks are associated with calculated shear stress increases, while ∼39% are associated with shear stress decreases. If earthquakes associated with calculated shear stress increases are interpreted as triggered, then such events make up at least 8% of the CMT catalog. Globally, these triggered earthquakes obey an Omori law rate decay that lasts between ∼7–11 years after the main shock. Earthquakes associated with calculated shear stress increases occur at higher rates than background up to 240 km away from the main shock centroid. Omori's law is one of the few time-predictable patterns evident in the global occurrence of earthquakes. If large triggered earthquakes habitually obey Omori's law, then their hazard can be more readily assessed. The characteristic rate change with time and spatial distribution can be used to rapidly assess the likelihood of triggered earthquakes following events of Ms ≥ 7.0. I show an example application to the M = 7.7 13 January 2001 El Salvador earthquake where use of global statistics appears to provide a better rapid hazard estimate than Coulomb stress change calculations. date: 2002-09-25 date_type: published publication: Journal of Geophysical Research volume: 107 number: B9 publisher: American Geophysical Union pagerange: 1-19 id_number: doi:10.1029/2001JB000646 refereed: TRUE issn: 0148-0227 official_url: http://dx.doi.org/10.1029/2001JB000646 access_IS-EPOS: limited owner: Publisher citation: Parsons, Tom (2002) Global Omori law decay of triggered earthquakes: Large aftershocks outside the classical aftershock zone. Journal of Geophysical Research, 107 (B9). pp. 1-19. DOI: https://doi.org/10.1029/2001JB000646