{"@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/1360855569437123712.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1126/science.281.5380.1175"}},{"identifier":{"@type":"URI","@value":"https://www.science.org/doi/pdf/10.1126/science.281.5380.1175"}}],"dc:title":[{"@value":"Variation of Interplate Fault Zone Properties with Depth in the Japan Subduction Zone"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>The depth dependence of physical properties along the Japan subduction zone interface was explored using teleseismic recordings of earthquake signals. Broadband body waves were inverted to determine the duration of rupture and source depth for 40 interplate thrust earthquakes located offshore of Honshu between 1989 and 1995. After scaling for differences in seismic moment, there is a systematic decrease in rupture duration with increasing depth along the subducting plate interface. This indicates increases in rupture velocity or stress drop with depth, likely related to variation in rigidity of sediments on the megathrust.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380855569437123712","@type":"Researcher","foaf:name":[{"@value":"Susan L. Bilek"}],"jpcoar:affiliationName":[{"@value":"Institute of Tectonics and Earth Sciences Department, University of California, Santa Cruz, CA 95064, USA."}]},{"@id":"https://cir.nii.ac.jp/crid/1380855569437123713","@type":"Researcher","foaf:name":[{"@value":"Thorne Lay"}],"jpcoar:affiliationName":[{"@value":"Institute of Tectonics and Earth Sciences Department, University of California, Santa Cruz, CA 95064, 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":"1998-08-21","prism:volume":"281","prism:number":"5380","prism:startingPage":"1175","prism:endingPage":"1178"},"reviewed":"false","url":[{"@id":"https://www.science.org/doi/pdf/10.1126/science.281.5380.1175"}],"createdAt":"2002-07-27","modifiedAt":"2024-01-13","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050285299729401344","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Source Modeling of an Mw5.9 Earthquake in the Nankai Trough, Southwest Japan, Using Offshore and Onshore Strong‐Motion Waveform Records"}]},{"@id":"https://cir.nii.ac.jp/crid/1050587981432203904","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Stress drops for intermediate-depth intraslab earthquakes beneath Hokkaido, northern Japan: Differences between the subducting oceanic crust and mantle events"},{"@value":"Stress drops for intermediate‐depth intraslab earthquakes beneath <scp>H</scp>okkaido, northern <scp>J</scp>apan: Differences between the subducting oceanic crust and mantle events"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004236003004416","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Laboratory measurements quantifying elastic properties of accretionary wedge sediments: Implications for slip to the trench during the 2011 Mw 9.0 Tohoku-Oki earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360580229812451840","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The Mw 6.0–6.8 Quasi‐Repeating Earthquakes Off Miyagi, Japan, With Variable Moment Release Patterns Due To a Hidden Adjacent Slip Patch"}]},{"@id":"https://cir.nii.ac.jp/crid/2051996267023640576","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Frictional properties of sediments entering the Costa Rica subduction zone offshore the Osa Peninsula : implications for fault slip in shallow subduction zones"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1126/science.281.5380.1175"},{"@type":"CROSSREF","@value":"10.1130/ges01630.1_references_DOI_UqwaarxMgC6AEgQjwiIM17smhKe"},{"@type":"CROSSREF","@value":"10.1785/0120170357_references_DOI_UqwaarxMgC6AEgQjwiIM17smhKe"},{"@type":"CROSSREF","@value":"10.1186/1880-5981-66-72_references_DOI_UqwaarxMgC6AEgQjwiIM17smhKe"},{"@type":"CROSSREF","@value":"10.1029/2022jb025654_references_DOI_UqwaarxMgC6AEgQjwiIM17smhKe"},{"@type":"CROSSREF","@value":"10.1002/2014gc005603_references_DOI_UqwaarxMgC6AEgQjwiIM17smhKe"}]}