{"@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/1361981470777639552.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1126/science.1256074"}},{"identifier":{"@type":"URI","@value":"https://www.science.org/doi/pdf/10.1126/science.1256074"}}],"dc:title":[{"@value":"Intense foreshocks and a slow slip event preceded the 2014 Iquique\n            <i>M</i>\n            <sub>w</sub>\n            8.1 earthquake"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>The earthquake that rocked northern Chile</jats:title>\n          <jats:p>\n            Subduction zones often produce the largest earthquakes on Earth. A magnitude 8.2 earthquake (Iquique) occurred in one such zone off the coast of northern Chile on 1 April 2014, in a seismic gap that had not experienced a large earthquake since the 9.0 one in 1877. Ruiz\n            <jats:italic>et al.</jats:italic>\n            analyzed continuous GPS data to monitor the movement of plates over time in this region, including before and after major earthquakes. The most recent large quake was preceded by an extended series of smaller earthquakes and creeping westward movement of the coastline.\n          </jats:p>\n          <jats:p>\n            <jats:italic>Science</jats:italic>\n            , this issue p.\n            <jats:related-article xmlns:xlink=\"http://www.w3.org/1999/xlink\" ext-link-type=\"doi\" issue=\"6201\" page=\"1165\" related-article-type=\"in-this-issue\" vol=\"345\" xlink:href=\"10.1126/science.1256074\">1165</jats:related-article>\n          </jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380005518374547210","@type":"Researcher","foaf:name":[{"@value":"S. Ruiz"}],"jpcoar:affiliationName":[{"@value":"Departamento de Geofísica, Facultad de Ciencias Físicas y Matemáticas, Universidad de Chile, Santiago, Chile."}]},{"@id":"https://cir.nii.ac.jp/crid/1381981470777639556","@type":"Researcher","foaf:name":[{"@value":"M. Metois"}],"jpcoar:affiliationName":[{"@value":"Istituto Nazionale di Geofisica e Vulcanologia, Centro Nazionale Terremoti, Rome, Italy."}]},{"@id":"https://cir.nii.ac.jp/crid/1381981470777639554","@type":"Researcher","foaf:name":[{"@value":"A. Fuenzalida"}],"jpcoar:affiliationName":[{"@value":"School of Environmental Sciences, University of Liverpool, Liverpool, UK."}]},{"@id":"https://cir.nii.ac.jp/crid/1381981470777639555","@type":"Researcher","foaf:name":[{"@value":"J. Ruiz"}],"jpcoar:affiliationName":[{"@value":"Departamento de Geofísica, Facultad de Ciencias Físicas y Matemáticas, Universidad de Chile, Santiago, Chile."}]},{"@id":"https://cir.nii.ac.jp/crid/1381981470777639559","@type":"Researcher","foaf:name":[{"@value":"F. Leyton"}],"jpcoar:affiliationName":[{"@value":"Centro Sismológico Nacional, Facultad de Ciencias Físicas y Matemáticas, Universidad de Chile, Santiago, Chile."}]},{"@id":"https://cir.nii.ac.jp/crid/1381981470777639553","@type":"Researcher","foaf:name":[{"@value":"R. Grandin"}],"jpcoar:affiliationName":[{"@value":"Institut de Physique du Globe de Paris, Sorbonne Paris Cité, Université Paris Diderot, UMR 7154 CNRS, Paris, France."}]},{"@id":"https://cir.nii.ac.jp/crid/1381981470777639557","@type":"Researcher","foaf:name":[{"@value":"C. Vigny"}],"jpcoar:affiliationName":[{"@value":"Laboratoire de Geologie, UMR 8538 CNRS Ecole Normale Superieure, Paris, France."}]},{"@id":"https://cir.nii.ac.jp/crid/1381981470777639552","@type":"Researcher","foaf:name":[{"@value":"R. Madariaga"}],"jpcoar:affiliationName":[{"@value":"Laboratoire de Geologie, UMR 8538 CNRS Ecole Normale Superieure, Paris, France."}]},{"@id":"https://cir.nii.ac.jp/crid/1381981470777639558","@type":"Researcher","foaf:name":[{"@value":"J. Campos"}],"jpcoar:affiliationName":[{"@value":"Departamento de Geofísica, Facultad de Ciencias Físicas y Matemáticas, Universidad de Chile, Santiago, Chile."}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00368075"},{"@type":"EISSN","@value":"10959203"}],"prism:publicationName":[{"@value":"Science"}],"dc:publisher":[{"@value":"American Association for the Advancement of Science (AAAS)"}],"prism:publicationDate":"2014-09-05","prism:volume":"345","prism:number":"6201","prism:startingPage":"1165","prism:endingPage":"1169"},"reviewed":"false","url":[{"@id":"https://www.science.org/doi/pdf/10.1126/science.1256074"}],"createdAt":"2014-07-25","modifiedAt":"2024-01-10","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050001339107234432","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Connecting slow earthquakes to huge earthquakes"},{"@value":"Connecting slow earthquakes 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