{"@context":{"@vocab":"https://cir.nii.ac.jp/schema/1.0/","rdfs":"http://www.w3.org/2000/01/rdf-schema#","dc":"http://purl.org/dc/elements/1.1/","dcterms":"http://purl.org/dc/terms/","foaf":"http://xmlns.com/foaf/0.1/","prism":"http://prismstandard.org/namespaces/basic/2.0/","cinii":"http://ci.nii.ac.jp/ns/1.0/","datacite":"https://schema.datacite.org/meta/kernel-4/","ndl":"http://ndl.go.jp/dcndl/terms/","jpcoar":"https://github.com/JPCOAR/schema/blob/master/2.0/"},"@id":"https://cir.nii.ac.jp/crid/1361699993537286144.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1002/2013jb010259"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2F2013JB010259"}},{"identifier":{"@type":"URI","@value":"https://onlinelibrary.wiley.com/doi/pdf/10.1002/2013JB010259"}},{"identifier":{"@type":"URI","@value":"https://onlinelibrary.wiley.com/doi/full-xml/10.1002/2013JB010259"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1002/2013JB010259"}}],"dc:title":[{"@value":"Quantitative description of induced seismic activity before and after the 2011 Tohoku‐Oki earthquake by nonstationary ETAS models"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>The epidemic‐type aftershock sequence (ETAS) model is extended for application to nonstationary seismic activity, including transient swarm activity or seismicity anomalies, in a seismogenic region. The time‐dependent rates of both background seismicity and aftershock productivity in the ETAS model are optimally estimated from hypocenter data. These rates can provide quantitative evidence for abrupt or gradual changes in shear stress and/or fault strength due to aseismic transient causes such as triggering by remote earthquakes, slow slips, or fluid intrusions within the region. This extended model is applied to data sets from several seismic events including swarms that were induced by the <jats:italic>M</jats:italic>9.0 Tohoku‐Oki earthquake of 2011.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1381699993537286145","@type":"Researcher","foaf:name":[{"@value":"Takao Kumazawa"}],"jpcoar:affiliationName":[{"@value":"The Institute of Statistical Mathematics  Tachikawa Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1381699993537286144","@type":"Researcher","foaf:name":[{"@value":"Yosihiko Ogata"}],"jpcoar:affiliationName":[{"@value":"The Institute of Statistical Mathematics  Tachikawa Japan"},{"@value":"Institute of Industrial Science University of Tokyo  Meguro‐ku Japan"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"21699313"},{"@type":"EISSN","@value":"21699356"}],"prism:publicationName":[{"@value":"Journal of Geophysical Research: Solid Earth"}],"dc:publisher":[{"@value":"American Geophysical Union 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