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dc.contributor.authorSiino, Marianna
dc.contributor.authoradelfio, giada
dc.contributor.authorMateu, Jorge
dc.contributor.authorCHIODI, Marcello
dc.contributor.authorD’Alessandro, Antonino
dc.date.accessioned2018-01-23T19:41:51Z
dc.date.available2018-01-23T19:41:51Z
dc.date.issued2017
dc.identifier.citationSiino, M., Adelfio, G., Mateu, J., Chiodi, M., & D’Alessandro, A. (2017). Spatial pattern analysis using hybrid models: an application to the Hellenic seismicity. Stochastic Environmental Research and Risk Assessment, 31(7), 1633-1648.ca_CA
dc.identifier.issn1436-3240
dc.identifier.issn1436-3256
dc.identifier.urihttp://hdl.handle.net/10234/172172
dc.description.abstractEarthquakes are one of the most destructive natural disasters and the spatial distribution of their epi- centres generally shows diverse interaction structures at different spatial scales. In this paper, we use a multi-scale point pattern model to describe the main seismicity in the Hellenic area over the last 10 years. We analyze the interaction between events and the relationship with geo- logical information of the study area, using hybrid models as proposed by Baddeley et al. ( 2013 ). In our analysis, we find two competing suitable hybrid models, one with a full parametric structure and the other one based on nonpara- metric kernel estimators for the spatial inhomogeneity.ca_CA
dc.format.extent16 p.ca_CA
dc.format.mimetypeapplication/pdfca_CA
dc.language.isoengca_CA
dc.publisherSpringer Verlagca_CA
dc.relation.isPartOfStochastic Environmental Research and Risk Assessment, 2017, vol. 31, no 7, p. 1633-1648.ca_CA
dc.rights© Springer-Verlag Berlin Heidelberg 2016ca_CA
dc.rights.urihttp://rightsstatements.org/vocab/InC/1.0/*
dc.subjecthellenic earthquakesca_CA
dc.subjecthybrids of gibbs point processesca_CA
dc.subjectpoint process residualsca_CA
dc.subjectspatial covariatesca_CA
dc.subjectspatial point processesca_CA
dc.titleSpatial pattern analysis using hybrid models: an application to the Hellenic seismicityca_CA
dc.typeinfo:eu-repo/semantics/articleca_CA
dc.identifier.doihttp://dx.doi.org/10.1007/s00477-016-1294-7
dc.relation.projectIDThis research was partially developed during the traineeship at the Istituto Nazionale di Geofisica e Vulcanologia funded by ‘‘PROGRAMMA OPERATIVO CONVERGENZA 2007-2013 FONDO SOCIALE EUROPEO (MISURA 3)’’ and this work was partially funded by Grant MTM2013-43917-P from the Spanish Ministry of Science and Education.ca_CA
dc.rights.accessRightsinfo:eu-repo/semantics/restrictedAccessca_CA
dc.relation.publisherVersionhttps://link.springer.com/article/10.1007/s00477-016-1294-7ca_CA
dc.type.versioninfo:eu-repo/semantics/publishedVersionca_CA


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