{"@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/1360283693141019904.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1111/iar.12179"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fiar.12179"}},{"identifier":{"@type":"URI","@value":"https://onlinelibrary.wiley.com/doi/pdf/10.1111/iar.12179"}}],"resourceType":"学術雑誌論文(journal article)","dc:title":[{"@value":"Evolution of crustal deformation in the northeast–central Japanese island arc: Insights from fault activity"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Abstract</jats:title><jats:p>We evaluated fault activity in northeast–central Japan based on fault orientation, regional stress field, and slip tendency analysis for active and non‐active faults (i.e. faults for which Quaternary activity has not been identified). Slip tendency is generally higher along active faults than non‐active faults, although a high slip tendency was observed along some non‐active faults, indicating their potential to become active. The potential for fault activity along non‐active faults can be modeled using the temporal evolution from non‐active to active during long‐term crustal deformation. The density of potentially active faults varies spatially across the study areas and reflects the temporal evolution of crustal deformation in northeast–central Japan.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1420845751140941312","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"50611191"},{"@type":"NRID","@value":"1000050611191"},{"@type":"NRID","@value":"9000006340479"},{"@type":"NRID","@value":"9000291604881"},{"@type":"NRID","@value":"9000347362352"},{"@type":"NRID","@value":"9000398390199"},{"@type":"NRID","@value":"9000243881702"},{"@type":"NRID","@value":"9000413515762"},{"@type":"NRID","@value":"9000242120224"},{"@type":"NRID","@value":"9000413482554"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/miyakawa-a"}],"foaf:name":[{"@value":"Ayumu Miyakawa"}],"jpcoar:affiliationName":[{"@value":"Geological Survey of Japan  Tsukuba 305‐8567 Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380847871317971200","@type":"Researcher","foaf:name":[{"@value":"Makoto Otsubo"}],"jpcoar:affiliationName":[{"@value":"Geological Survey of Japan  Tsukuba 305‐8567 Japan"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"10384871"},{"@type":"EISSN","@value":"14401738"}],"prism:publicationName":[{"@value":"Island Arc"}],"dc:publisher":[{"@value":"Wiley"}],"prism:publicationDate":"2017-02-08","prism:volume":"26","prism:number":"2","prism:startingPage":"e12179"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","dc:rights":["http://creativecommons.org/licenses/by/4.0/"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fiar.12179"},{"@id":"https://onlinelibrary.wiley.com/doi/pdf/10.1111/iar.12179"}],"createdAt":"2017-02-08","modifiedAt":"2023-10-02","project":[{"@id":"https://cir.nii.ac.jp/crid/1040000782279195392","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"26109003"},{"@type":"JGN","@value":"JP26109003"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PLANNED-26109003/"}],"notation":[{"@language":"ja","@value":"異なる時空間スケールにおける日本列島の変形場の解明"},{"@language":"en","@value":"Resolution of crustal deformation of the Japan Islands in various spatio-temporal 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