{"@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/1363670320203985280.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1007/s00024-018-1828-7"}},{"identifier":{"@type":"URI","@value":"http://link.springer.com/article/10.1007/s00024-018-1828-7/fulltext.html"}},{"identifier":{"@type":"URI","@value":"http://link.springer.com/content/pdf/10.1007/s00024-018-1828-7.pdf"}}],"dc:title":[{"@value":"Estimating Q Factor from Multi-mode Shallow-Seismic Surface Waves"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1383670320203985283","@type":"Researcher","foaf:name":[{"@value":"Lingli Gao"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670320203985282","@type":"Researcher","foaf:name":[{"@value":"Yudi Pan"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670320203985280","@type":"Researcher","foaf:name":[{"@value":"Gang Tian"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670320203985281","@type":"Researcher","foaf:name":[{"@value":"Jianghai Xia"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00334553"},{"@type":"EISSN","@value":"14209136"}],"prism:publicationName":[{"@value":"Pure and Applied Geophysics"}],"dc:publisher":[{"@value":"Springer Science and Business Media LLC"}],"prism:publicationDate":"2018-03-16","prism:volume":"175","prism:number":"8","prism:startingPage":"2609","prism:endingPage":"2622"},"reviewed":"false","dc:rights":["http://www.springer.com/tdm"],"url":[{"@id":"http://link.springer.com/article/10.1007/s00024-018-1828-7/fulltext.html"},{"@id":"http://link.springer.com/content/pdf/10.1007/s00024-018-1828-7.pdf"}],"createdAt":"2018-03-16","modifiedAt":"2019-03-15","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360290617579222144","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Limits and Benefits of the Spatial Autocorrelation Microtremor Array Method Due to the Incoherent Noise, With Special Reference to the Analysis of Long Wavelength Ranges"}]},{"@id":"https://cir.nii.ac.jp/crid/2051996266992054400","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Array-size dependency of the upper limit wavelength normalized by array radius for the standard spatial autocorrelation method"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1007/s00024-018-1828-7"},{"@type":"CROSSREF","@value":"10.1029/2020jb019850_references_DOI_1d28UxBzkX6sToHfvoMjhxo4jmT"},{"@type":"CROSSREF","@value":"10.1186/s40623-022-01641-2_references_DOI_1d28UxBzkX6sToHfvoMjhxo4jmT"}]}