{"@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/1360011142938534016.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1016/j.epsl.2020.116143"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0012821X20300868?httpAccept=text/xml"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0012821X20300868?httpAccept=text/plain"}}],"dc:title":[{"@value":"Plate geometry model and seismicity in the northern Ryukyu subduction zone, Japan, deduced from amphibious seismic observations"}],"description":[{"notation":[{"@value":"Abstract   In this study, the geometry of the subducted Philippine Sea Plate interface beneath the northern Ryukyu Trench subduction zone was estimated based on seismic tomography and focal mechanism estimations using passive data obtained from a temporary amphibious seismic network and permanent land stations. Using relocated low-angle thrust-type earthquakes and information obtained from previous studies, we constrained the plate geometry from the trench axis to a depth of 60 km with uncertainties of"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380011142938534020","@type":"Researcher","foaf:name":[{"@value":"Yojiro Yamamoto"}]},{"@id":"https://cir.nii.ac.jp/crid/1380011142938534144","@type":"Researcher","foaf:name":[{"@value":"Tsutomu Takahashi"}]},{"@id":"https://cir.nii.ac.jp/crid/1380011142938534016","@type":"Researcher","foaf:name":[{"@value":"Yasushi Ishihara"}]},{"@id":"https://cir.nii.ac.jp/crid/1380011142938534018","@type":"Researcher","foaf:name":[{"@value":"Koichiro Obana"}]},{"@id":"https://cir.nii.ac.jp/crid/1380011142938534145","@type":"Researcher","foaf:name":[{"@value":"Seiichi Miura"}]},{"@id":"https://cir.nii.ac.jp/crid/1380011142938534019","@type":"Researcher","foaf:name":[{"@value":"Shuichi Kodaira"}]},{"@id":"https://cir.nii.ac.jp/crid/1380011142938534017","@type":"Researcher","foaf:name":[{"@value":"Yoshiyuki Kaneda"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"0012821X"}],"prism:publicationName":[{"@value":"Earth and Planetary Science Letters"}],"dc:publisher":[{"@value":"Elsevier BV"}],"prism:publicationDate":"2020-04","prism:volume":"536","prism:startingPage":"116143"},"reviewed":"false","dc:rights":["https://www.elsevier.com/tdm/userlicense/1.0/","https://www.elsevier.com/legal/tdmrep-license"],"url":[{"@id":"https://api.elsevier.com/content/article/PII:S0012821X20300868?httpAccept=text/xml"},{"@id":"https://api.elsevier.com/content/article/PII:S0012821X20300868?httpAccept=text/plain"}],"createdAt":"2020-02-12","modifiedAt":"2025-11-02","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360025030626632064","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Seismic activity around shallow plate boundary near westernmost Nankai Trough revealed by ocean bottom seismometer observation"}]},{"@id":"https://cir.nii.ac.jp/crid/1360572092541173504","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Rejuvenated extension of the Philippine Sea plate and its effect on subduction dynamics in the Nankai Trough"}]},{"@id":"https://cir.nii.ac.jp/crid/2051996266990518912","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Seismicity distribution in the Tonankai and Nankai seismogenic zones and its spatiotemporal relationship with interplate coupling and slow earthquakes"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1016/j.epsl.2020.116143"},{"@type":"OPENAIRE","@value":"doi_dedup___::14391c74d44d0a9f6bcd11c25396fc93"},{"@type":"CROSSREF","@value":"10.1186/s40623-024-02122-4_references_DOI_NLPPTJgQTbd55ZV4lyiHWWSUsy0"},{"@type":"CROSSREF","@value":"10.1111/iar.12402_references_DOI_NLPPTJgQTbd55ZV4lyiHWWSUsy0"},{"@type":"CROSSREF","@value":"10.1186/s40645-022-00493-4_references_DOI_NLPPTJgQTbd55ZV4lyiHWWSUsy0"}]}