{"@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/1360005520966852736.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1126/science.aax5618"}},{"identifier":{"@type":"URI","@value":"https://syndication.highwire.org/content/doi/10.1126/science.aax5618"}},{"identifier":{"@type":"URI","@value":"https://www.science.org/doi/pdf/10.1126/science.aax5618"}},{"identifier":{"@type":"PMID","@value":"31439780"}}],"resourceType":"学術雑誌論文(journal article)","dc:title":[{"@value":"The slow earthquake spectrum in the Japan Trench illuminated by the S-net seafloor observatories"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Slow earthquake segmentation</jats:title>\n          <jats:p>\n            The Japan Trench is responsible for disastrous megathrust earthquakes like the 2011 Tohoku-Oki quake. Nishikawa\n            <jats:italic>et al.</jats:italic>\n            used new observations from the S-net ocean-bottom seismic network to map slow earthquakes—disturbances that do not cause ground shaking—along the Japan Trench (see the Perspective by Houston). They found that the area that ruptured during the 2011 quake was bounded by areas that have large numbers of slow earthquakes. A segmentation likely caused the 2011 rupture to cease, an observation that is important for assessing risk from future major earthquakes.\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=\"6455\" page=\"808\" related-article-type=\"in-this-issue\" vol=\"365\" xlink:href=\"10.1126/science.aax5618\">808</jats:related-article>\n            ; see also p.\n            <jats:related-article xmlns:xlink=\"http://www.w3.org/1999/xlink\" ext-link-type=\"doi\" issue=\"6455\" page=\"750\" related-article-type=\"in-this-issue\" vol=\"365\" xlink:href=\"10.1126/science.aay5621\">750</jats:related-article>\n          </jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380005520966852736","@type":"Researcher","foaf:name":[{"@value":"T. Nishikawa"}],"jpcoar:affiliationName":[{"@value":"Disaster Prevention Research Institute, Kyoto University, Uji, Japan."}]},{"@id":"https://cir.nii.ac.jp/crid/1380005520966852610","@type":"Researcher","foaf:name":[{"@value":"T. Matsuzawa"}],"jpcoar:affiliationName":[{"@value":"National Research Institute for Earth Science and Disaster Resilience, Tsukuba, Japan."}]},{"@id":"https://cir.nii.ac.jp/crid/1380005520966852608","@type":"Researcher","foaf:name":[{"@value":"K. Ohta"}],"jpcoar:affiliationName":[{"@value":"Disaster Prevention Research Institute, Kyoto University, Uji, Japan."}]},{"@id":"https://cir.nii.ac.jp/crid/1380005520966852737","@type":"Researcher","foaf:name":[{"@value":"N. Uchida"}],"jpcoar:affiliationName":[{"@value":"Graduate School of Science and International Research Institute of Disaster Science, Tohoku University, Sendai, Japan."}]},{"@id":"https://cir.nii.ac.jp/crid/1380005520966852864","@type":"Researcher","foaf:name":[{"@value":"T. Nishimura"}],"jpcoar:affiliationName":[{"@value":"Disaster Prevention Research Institute, Kyoto University, Uji, Japan."}]},{"@id":"https://cir.nii.ac.jp/crid/1380005520966852609","@type":"Researcher","foaf:name":[{"@value":"S. Ide"}],"jpcoar:affiliationName":[{"@value":"Department of Earth and Planetary Science, University of Tokyo, Tokyo, Japan."}]}],"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":"2019-08-23","prism:volume":"365","prism:number":"6455","prism:startingPage":"808","prism:endingPage":"813"},"reviewed":"false","url":[{"@id":"https://syndication.highwire.org/content/doi/10.1126/science.aax5618"},{"@id":"https://www.science.org/doi/pdf/10.1126/science.aax5618"}],"createdAt":"2019-09-03","modifiedAt":"2024-01-15","project":[{"@id":"https://cir.nii.ac.jp/crid/1040000781844885248","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"15K05260"},{"@type":"JGN","@value":"JP15K05260"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-15K05260/"}],"notation":[{"@language":"ja","@value":"日本海溝海底地震津波観測網を用いた浅部プレート境界の非地震性すべり過程の解明"},{"@language":"en","@value":"Study on aseismic slip on the shallow plate interface by the S-net cabled 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