{"@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/1360002214349470592.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1002/2014tc003531"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2F2014TC003531"}}],"resourceType":"学術雑誌論文(journal article)","dc:title":[{"@value":"Middle Miocene swift migration of the TTT triple junction and rapid crustal growth in southwest Japan: A review"}],"dcterms:alternative":[{"@value":"Middle Miocene tectonics in SW Japan"}],"description":[{"notation":[{"@value":"We review recent progress in geological and geophysical investigation in SW Japan, Nankai Trough, and Philippine Sea Plate (PSP), and propose a hypothesis for the Miocene tectonics in SW Japan driven by middle Miocene swift migration of the TTT (trench-trench-trench) triple junction. The new hypothesis is based on the new interpretations as follows. Near-trench magmatism in the outer zone of SW Japan is ascribed to a collision of proto-Izu arc in addition to the previous model of an oceanic ridge of the Shikoku Basin and hot PSP subduction. The indentation structures at Capes Ashizuri, Muroto in Shikoku, and Shiono on the Kii Peninsula were previously explained by “kink folding” due to recent E-W compression. We alternatively suppose the collision of the active arc or topographic peaks such as seamounts inferred from geological and experimental observations. The main crustal component in SW Japan is suggested to be of igneous plutonic rocks rather than the previous interpretation of Cretaceous to Tertiary accretionary complexes. This is typically illustrated in the outer zone to the north of Capes Ashizuri, Muroto, and Shiono from geophysical observation of gravity anomalies, velocity and resistivity, together with geological estimations of caldera age and the size of its root pluton. Episodic crustal growth due to intrusion of igneous rock and subduction of the PSP may have stopped after approximately 12 Ma and restarted at approximately 6 Ma. Our emphasis for this gap is a cessation and resurgence of subduction rather than the previous interpretation, i.e., decreasing of subduction rate."}]}],"creator":[{"@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 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Koge"}],"jpcoar:affiliationName":[{"@value":"Department of Earth and Planetary Science, Graduate School of Science; University of Tokyo; Tokyo Japan"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"02787407"}],"prism:publicationName":[{"@value":"Tectonics"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"2014-06-30","prism:volume":"33","prism:number":"7","prism:startingPage":"1219","prism:endingPage":"1238"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","dc:rights":["http://doi.wiley.com/10.1002/tdm_license_1.1"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2F2014TC003531"}],"createdAt":"2014-06-06","modifiedAt":"2024-05-27","project":[{"@id":"https://cir.nii.ac.jp/crid/1040000782144521216","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"23244099"},{"@type":"JGN","@value":"JP23244099"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-23244099/"}],"notation":[{"@language":"ja","@value":"沈み込み地震発生分岐断層の断層メカニズムとその進化"},{"@language":"en","@value":"Fault mechanism and evolution of the seismogenic splay fault in subduction zone"}]},{"@id":"https://cir.nii.ac.jp/crid/1040000782271961984","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"25800278"},{"@type":"JGN","@value":"JP25800278"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-25800278/"}],"notation":[{"@language":"ja","@value":"カッティングスを用いた南海トラフ巨大分岐断層活動史の解明"},{"@language":"en","@value":"Cuttings-based research for assessing evolution of the megasplay fault in the Nankai Trough"}]},{"@id":"https://cir.nii.ac.jp/crid/1040282257174478592","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"24340125"},{"@type":"JGN","@value":"JP24340125"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-24340125/"}],"notation":[{"@language":"ja","@value":"沈み込みプレート境界における有効摩擦係数の地震サイクルに伴う時空間変化"},{"@language":"en","@value":"Time-spacio change in effective friction coefficient with seismic cycle in subduction zones"}]}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050289532527693952","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Geometrical dependence on the stress and slip tendency acting on the subduction megathrust of Nankai seismogenic zone off Kumano"},{"@value":"Geometrical dependence on the stress and slip tendency acting on the subduction megathrust of the Nankai seismogenic zone off Kumano"}]},{"@id":"https://cir.nii.ac.jp/crid/1050866117150510336","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Deep plutonic bodies over low-frequency earthquakes revealed from receiver-side Green's functions"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002215916314624","@type":"Article","resourceType":"学術雑誌論文(journal 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