Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/12623
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dc.date.accessioned2019-04-02T08:02:22Zen
dc.date.available2019-04-02T08:02:22Zen
dc.date.issued2018en
dc.identifier.urihttp://hdl.handle.net/2122/12623en
dc.description.abstractThe most popular aftershock forecasting model is based on the modified Omori law (MOL), which describes the expected decay of the aftershock given the mainshock’s magnitude. Although such a model is still widely used for operational purposes, it is not unusual that one or more aftershocks break the MOL behavior. In this case, the time evolution of the aftershock sequence becomes much more complicated, and it may be better described by more advanced models, which also account for the triggering capability of all aftershocks. The purpose of this work is to analyze deductively the conditions under which the mean trend of an aftershock sequence, generated by one single mainshock according to the MOL, is satisfactorily described by an inverse power law. Practically, this analysis provides the likelihood that an aftershock sequence will conform to one single MOL; that is, the likelihood of delivering reliable forecasts using a model based on a single MOL. Specifically, we analyze which conditions are present when the triggering capability of a selected aftershock significantly affects the aftershock rate caused by the mainshock. For example, we discuss the application of this scheme to sequences that either conform, or do not, to the MOL behavior, such as the Amatrice– Norcia (Italy 2016–2017), Emilia (Italy 2012), and Tohoku-Oki (Japan 2011) aftershock sequences.en
dc.language.isoEnglishen
dc.relation.ispartofSeismological Research Lettersen
dc.relation.ispartofseries3/89(2018)en
dc.titleHow Likely Does an Aftershock Sequence Conform to a Single Omori Law Behavior?en
dc.typearticleen
dc.description.statusPublisheden
dc.description.pagenumber1118-1128en
dc.identifier.doi10.1785/0220170224en
dc.description.obiettivoSpecifico6T. Studi di pericolosità sismica e da maremotoen
dc.description.journalTypeJCR Journalen
dc.contributor.authorSpassiani, Ilariaen
dc.contributor.authorMarzocchi, Warneren
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italiaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italiaen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextrestricted-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italia-
crisitem.author.orcid0000-0003-2252-0202-
crisitem.author.orcid0000-0002-9114-1516-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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