{"@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/1363670319851523328.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1126/science.1224030"}},{"identifier":{"@type":"URI","@value":"https://www.science.org/doi/pdf/10.1126/science.1224030"}}],"dc:title":[{"@value":"Earthquake in a Maze: Compressional Rupture Branching During the 2012\n            <i>M</i>\n            <sub>w</sub>\n            8.6 Sumatra Earthquake"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Earthquake in a Maze</jats:title>\n          <jats:p>\n            The 11 April 2012 magnitude 8.6 earthquake offshore of Sumatra was the largest measured earthquake along a strike-slip boundary that modern seismological instruments have ever recorded. Despite its size and proximity to a large population, there was no subsequent tsunami and there were no reported fatalities.\n            <jats:bold>\n              Meng\n              <jats:italic>et al.</jats:italic>\n            </jats:bold>\n            (p.\n            <jats:related-article xmlns:xlink=\"http://www.w3.org/1999/xlink\" ext-link-type=\"doi\" page=\"724\" related-article-type=\"in-this-issue\" vol=\"337\" xlink:href=\"10.1126/science.1224030\">724</jats:related-article>\n            , published online 19 July) used teleseismic data from seismological networks in Japan and Europe to image the source of high-frequency radiation generated by the earthquake to understand the mechanics of this unique event. The resultant back projections showed that the earthquake slowly ruptured along a complex series of faults. The deeper-than-usual rupture path and large stress drop are both features that may not be unique to this earthquake, suggesting that regions in a similar tectonic environment may have the potential for more complex—or larger—intraplate earthquakes than might have been expected.\n          </jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380004057902569097","@type":"Researcher","foaf:name":[{"@value":"L. Meng"}],"jpcoar:affiliationName":[{"@value":"Seismological Laboratory, Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA 91125, USA."}]},{"@id":"https://cir.nii.ac.jp/crid/1383670319851523328","@type":"Researcher","foaf:name":[{"@value":"J.-P. Ampuero"}],"jpcoar:affiliationName":[{"@value":"Seismological Laboratory, Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA 91125, USA."}]},{"@id":"https://cir.nii.ac.jp/crid/1383670319851523329","@type":"Researcher","foaf:name":[{"@value":"J. Stock"}],"jpcoar:affiliationName":[{"@value":"Seismological Laboratory, Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA 91125, USA."}]},{"@id":"https://cir.nii.ac.jp/crid/1383670319851523333","@type":"Researcher","foaf:name":[{"@value":"Z. Duputel"}],"jpcoar:affiliationName":[{"@value":"Seismological Laboratory, Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA 91125, USA."}]},{"@id":"https://cir.nii.ac.jp/crid/1383670319851523331","@type":"Researcher","foaf:name":[{"@value":"Y. Luo"}],"jpcoar:affiliationName":[{"@value":"Seismological Laboratory, Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA 91125, USA."}]},{"@id":"https://cir.nii.ac.jp/crid/1383670319851523330","@type":"Researcher","foaf:name":[{"@value":"V. C. Tsai"}],"jpcoar:affiliationName":[{"@value":"Seismological Laboratory, Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA 91125, USA."}]}],"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":"2012-08-10","prism:volume":"337","prism:number":"6095","prism:startingPage":"724","prism:endingPage":"726"},"reviewed":"false","url":[{"@id":"https://www.science.org/doi/pdf/10.1126/science.1224030"}],"createdAt":"2012-07-24","modifiedAt":"2024-01-10","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050007846254914176","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Consecutive ruptures on a complex conjugate fault system during the 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