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dc.contributor.author Pulido, Nelson
dc.contributor.author Aguilar, Zenón
dc.contributor.author Tavera, Hernando
dc.contributor.author Chlieh, Mohamed
dc.contributor.author Calderón, Diana
dc.contributor.author Sekiguchi, Toru
dc.contributor.author Nakai, Shoichi
dc.contributor.author Yamazaki, Fumio
dc.date.accessioned 2018-09-10T18:31:37Z
dc.date.available 2018-09-10T18:31:37Z
dc.date.issued 2015-01
dc.identifier.govdoc index-oti2018
dc.identifier.issn 371106
dc.identifier.uri http://repositorio.igp.gob.pe/handle/IGP/2894
dc.description En: Bulletin of the Seismological Society of America v. 105, n. 1 (January 2015), p. 368-386. es_ES
dc.description.abstract "The 2011 moment magnitude (Mw) 9.0 Tohoku-Oki Japan earthquake occurred in a region where giant megathrust earthquakes were not expected. This earthquake proved the difficulty in assessing seismic hazard by relying mainly on information from historical and instrumental seismicity. To help improve the seismic-hazard assessment for such rare events, we propose a methodology to estimate the slip distribution of future megathrust earthquakes based on a model of interseismic coupling distribution in subduction margins, as well as information of historical earthquakes, and apply the method to the central Peru region, Lima. The slip model obtained from geodetic data represents the large scale features of asperities within the megathrust, which is appropriate for simulation of long-period waves and tsunami modeling. For the simulation of a broadband strong ground motion, we add small scale heterogeneities to the source slip to be able to simulate high frequencies. To achieve this purpose, we propose broadband source models constructed by adding short-wavelength slip distributions obtained from a Von Karman power spectral density function, to the slip model inferred from interseismic geodetic data. Using these slip models and assuming several hypocenter locations, we calculate a set of strong ground motions for Lima and incorporate site effects obtained from microtremors surveys and geotechnical data. Our simulated average pseudospectral accelerations (period 0.3 s) are above 1:5g for wide areas in Lima, which may be critical in terms of damage of low- to midrise masonry and reinforced concrete buildings, which characterize the majority of buildings in Lima." es_ES
dc.format application/pdf es_ES
dc.language.iso eng es_ES
dc.publisher Seismological Society of America es_ES
dc.relation.uri https://pubs.geoscienceworld.org/ssa/bssa/article-abstract/105/1/368/323556 es_ES
dc.rights info:eu-repo/semantics/restrictedAccess es_ES
dc.rights.uri info:eu-repo/semantics/restrictedAccess es_ES
dc.source Repositorio institucional - IGP es_ES
dc.subject Terremotos--Perú es_ES
dc.subject Geotecnia ambiental--Perú es_ES
dc.subject Sismometría es_ES
dc.subject Evaluación de riesgos es_ES
dc.subject Predicción de terremotos--Perú es_ES
dc.subject Localización de eventos sísmicos--Perú es_ES
dc.title Scenario source models and strong ground motion for future mega-earthquakes: Application to Lima, Central Peru es_ES
dc.type info:eu-repo/semantics/article es_ES
dc.subject.ocde Terremotos es_ES
dc.subject.ocde Evaluación es_ES
dc.subject.ocde Riesgo es_ES
dc.subject.ocde Perú es_ES
dc.subject.ocde Predicciones es_ES
dc.subject.ocde Geología es_ES
dc.identifier.journal Bulletin of the Seismological Society of America es_ES
dc.description.peer-review Por pares es_ES
dc.identifier.doi 10.1785/0120140098 es_ES

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