{"@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/1360004232135547264.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1016/j.epsl.2017.08.041"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0012821X17304946?httpAccept=text/xml"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0012821X17304946?httpAccept=text/plain"}}],"resourceType":"学術雑誌論文(journal article)","dc:title":[{"@value":"3D geometry of a plate boundary fault related to the 2016 Off-Mie earthquake in the Nankai subduction zone, Japan"}],"description":[{"notation":[{"@value":"Abstract   We used recent seismic data and advanced techniques to investigate 3D fault geometry over the transition from the partially coupled to the fully coupled plate interface inboard of the Nankai Trough off the Kii Peninsula, Japan. We found that a gently dipping plate boundary decollement with a thick underthrust layer extends beneath the entire Kumano forearc basin. The 1 April 2016 Off-Mie earthquake (Mw6.0) and its aftershocks occurred, where the plate boundary decollement steps down close to the oceanic crust surface. This location also lies beneath the trenchward edge of an older accretionary prism (∼14 Ma) developed along the coast of the Kii peninsula. The strike of the 2016 rupture plane was similar to that of a formerly active splay fault system in the accretionary prism. Thus, the fault planes of the 2016 earthquake and its aftershocks were influenced by the geometry of the plate interface as well as splay faulting. The 2016 earthquake occurred within the rupture area of large interplate earthquakes such as the 1944 Tonankai earthquake (Mw8.1), although the 2016 rupture area was much smaller than that of the 1944 event. Whereas the hypocenter of the 2016 earthquake was around the underplating sequence beneath the younger accretionary prism (∼6 Ma), the 1944 great earthquake hypocenter was close to oceanic crust surface beneath the older accretionary prism. The variation of fault geometry and lithology may influence the degree of coupling along the plate interface, and such coupling variation could hinder slip propagation toward the deeper plate interface in the 2016 event."}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380004232135547265","@type":"Researcher","foaf:name":[{"@value":"Takeshi Tsuji"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004232135547264","@type":"Researcher","foaf:name":[{"@value":"Shohei Minato"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004232135547267","@type":"Researcher","foaf:name":[{"@value":"Rie Kamei"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004232135547268","@type":"Researcher","foaf:name":[{"@value":"Tetsuro Tsuru"}]},{"@id":"https://cir.nii.ac.jp/crid/1420001326224587776","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"80153188"},{"@type":"NRID","@value":"1000080153188"},{"@type":"CINII_AUTHOR_ID","@value":"DA12254232"},{"@type":"URI","@value":"https://ci.nii.ac.jp/author/DA12254232#entity"},{"@type":"URI","@value":"https://viaf.org/viaf/NII%7CDA12254232"},{"@type":"NRID","@value":"9000004613729"},{"@type":"NRID","@value":"9000017071286"},{"@type":"NRID","@value":"9000020466429"},{"@type":"NRID","@value":"9000020954041"},{"@type":"NRID","@value":"9000018150199"},{"@type":"NRID","@value":"9000003377698"},{"@type":"NRID","@value":"9000004838510"},{"@type":"NRID","@value":"9000259288536"},{"@type":"NRID","@value":"9000255862908"},{"@type":"NRID","@value":"9000007639236"},{"@type":"NRID","@value":"9000006912115"},{"@type":"NRID","@value":"9000020665676"},{"@type":"NRID","@value":"9000403693862"},{"@type":"NRID","@value":"9000397649361"},{"@type":"NRID","@value":"9000002496992"},{"@type":"NRID","@value":"9000361706727"},{"@type":"NRID","@value":"9000018546677"},{"@type":"NRID","@value":"9000399947855"},{"@type":"NRID","@value":"9000008060173"},{"@type":"NRID","@value":"9000401508427"},{"@type":"NRID","@value":"9000003844860"},{"@type":"NRID","@value":"9000010333135"},{"@type":"NRID","@value":"9000254585631"},{"@type":"NRID","@value":"9000255797239"},{"@type":"NRID","@value":"9000000138994"},{"@type":"NRID","@value":"9000003818160"},{"@type":"NRID","@value":"9000356479532"},{"@type":"NRID","@value":"9000272993664"},{"@type":"NRID","@value":"9000253256638"},{"@type":"NRID","@value":"9000399156135"},{"@type":"NRID","@value":"9000017396195"},{"@type":"NRID","@value":"9000391402344"},{"@type":"NRID","@value":"9000007297732"},{"@type":"NRID","@value":"9000314388082"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/read0067865"}],"foaf:name":[{"@value":"Gaku Kimura"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"0012821X"}],"prism:publicationName":[{"@value":"Earth and Planetary Science Letters"}],"dc:publisher":[{"@value":"Elsevier BV"}],"prism:publicationDate":"2017-11","prism:volume":"478","prism:startingPage":"234","prism:endingPage":"244"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","dc:rights":["https://www.elsevier.com/tdm/userlicense/1.0/","https://www.elsevier.com/legal/tdmrep-license","http://creativecommons.org/licenses/by/4.0/"],"url":[{"@id":"https://api.elsevier.com/content/article/PII:S0012821X17304946?httpAccept=text/xml"},{"@id":"https://api.elsevier.com/content/article/PII:S0012821X17304946?httpAccept=text/plain"}],"createdAt":"2017-09-28","modifiedAt":"2025-09-15","project":[{"@id":"https://cir.nii.ac.jp/crid/1040000781827075840","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"15H02988"},{"@type":"JGN","@value":"JP15H02988"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-15H02988/"}],"notation":[{"@language":"ja","@value":"ターミナル海盆の堆積記録を用いた南海トラフの地震履歴の高精度化"},{"@language":"en","@value":"Accuracy improvement of earthquake history of the Nankai Trough by sediment records from terminal basins"}]},{"@id":"https://cir.nii.ac.jp/crid/1040000781958652032","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"17H05318"},{"@type":"JGN","@value":"JP17H05318"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PUBLICLY-17H05318/"}],"notation":[{"@language":"ja","@value":"断層進化過程の解明に向けた階層型デジタル岩石物理化学モデルの開発"},{"@language":"en","@value":"Investigation of fault evolution process using physicochemical simulation for digitalized rock models"}]},{"@id":"https://cir.nii.ac.jp/crid/1040282257416516864","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"15H05717"},{"@type":"JGN","@value":"JP15H05717"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-15H05717/"}],"notation":[{"@language":"ja","@value":"プレート境界断層超深度掘削・観測による南海トラフ巨大地震切迫度評価"},{"@language":"en","@value":"Urgency Evaluation of the Nankai Great Earthquake and Tsunami by Scientific Ocean 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