{"@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/1363670321256579968.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1126/sciadv.aav3274"}},{"identifier":{"@type":"URI","@value":"https://www.science.org/doi/pdf/10.1126/sciadv.aav3274"}}],"dc:title":[{"@value":"Slow slip events in the roots of the San Andreas fault"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>\n            By analyzing GPS time series, we have detected an averaged\n            <jats:italic>M</jats:italic>\n            <jats:sub>w</jats:sub>\n            4.9 slow slip event in the roots of the San Andreas fault.\n          </jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1383670321256579968","@type":"Researcher","foaf:name":[{"@value":"Baptiste Rousset"}],"jpcoar:affiliationName":[{"@value":"Department of Earth and Planetary Science, Berkeley Seismology Laboratory, University of California Berkeley, Berkeley, CA, USA."}]},{"@id":"https://cir.nii.ac.jp/crid/1383670321256579970","@type":"Researcher","foaf:name":[{"@value":"Roland Bürgmann"}],"jpcoar:affiliationName":[{"@value":"Department of Earth and Planetary Science, Berkeley Seismology Laboratory, University of California Berkeley, Berkeley, CA, USA."}]},{"@id":"https://cir.nii.ac.jp/crid/1383670321256579969","@type":"Researcher","foaf:name":[{"@value":"Michel Campillo"}],"jpcoar:affiliationName":[{"@value":"Institut des Sciences de la Terre, Université Grenoble Alpes, CNRS, IRD, Saint-Martin-d’Hères, France."},{"@value":"Department of Earth, Atmospheric, and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, MA, USA."}]}],"publication":{"publicationIdentifier":[{"@type":"EISSN","@value":"23752548"}],"prism:publicationName":[{"@value":"Science Advances"}],"dc:publisher":[{"@value":"American Association for the Advancement of Science (AAAS)"}],"prism:publicationDate":"2019-02","prism:volume":"5","prism:number":"2","prism:startingPage":"eaav3274"},"reviewed":"false","url":[{"@id":"https://www.science.org/doi/pdf/10.1126/sciadv.aav3274"}],"createdAt":"2019-02-14","modifiedAt":"2024-01-09","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050287606237344896","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Detailed Spatial Slip Distribution for Short‐Term Slow Slip Events Along the Nankai Subduction Zone, Southwest 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