{"@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/1363951796181748992.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1126/science.1070015"}},{"identifier":{"@type":"URI","@value":"https://www.science.org/doi/pdf/10.1126/science.1070015"}}],"dc:title":[{"@value":"Coda Wave Interferometry for Estimating Nonlinear Behavior in Seismic Velocity"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>In coda wave interferometry, one records multiply scattered waves at a limited number of receivers to infer changes in the medium over time. With this technique, we have determined the nonlinear dependence of the seismic velocity in granite on temperature and the associated acoustic emissions. This technique can be used in warning mode, to detect the presence of temporal changes in the medium, or in diagnostic mode, where the temporal change in the medium is quantified.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1383951796181748992","@type":"Researcher","foaf:name":[{"@value":"Roel Snieder"}],"jpcoar:affiliationName":[{"@value":"Department of Geophysics and Center for Wave Phenomena, Colorado School of Mines, Golden, CO 80401, USA."}]},{"@id":"https://cir.nii.ac.jp/crid/1383951796181748995","@type":"Researcher","foaf:name":[{"@value":"Alexandre Grêt"}],"jpcoar:affiliationName":[{"@value":"Department of Geophysics and Center for Wave Phenomena, Colorado School of Mines, Golden, CO 80401, USA."}]},{"@id":"https://cir.nii.ac.jp/crid/1383951796181748993","@type":"Researcher","foaf:name":[{"@value":"Huub Douma"}],"jpcoar:affiliationName":[{"@value":"Department of Geophysics and Center for Wave Phenomena, Colorado School of Mines, Golden, CO 80401, USA."}]},{"@id":"https://cir.nii.ac.jp/crid/1383951796181748994","@type":"Researcher","foaf:name":[{"@value":"John Scales"}],"jpcoar:affiliationName":[{"@value":"Department of Geophysics and Center for Wave Phenomena, Colorado School of Mines, Golden, CO 80401, 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":"2002-03-22","prism:volume":"295","prism:number":"5563","prism:startingPage":"2253","prism:endingPage":"2255"},"reviewed":"false","url":[{"@id":"https://www.science.org/doi/pdf/10.1126/science.1070015"}],"createdAt":"2002-07-27","modifiedAt":"2024-01-10","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360002216709700864","@type":"Article","resourceType":"学術雑誌論文(journal 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