{"@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/1360021390563077504.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1186/s40645-023-00578-8"}},{"identifier":{"@type":"URI","@value":"https://link.springer.com/content/pdf/10.1186/s40645-023-00578-8.pdf"}},{"identifier":{"@type":"URI","@value":"https://link.springer.com/article/10.1186/s40645-023-00578-8/fulltext.html"}}],"resourceType":"学術雑誌論文(journal article)","dc:title":[{"@value":"The nature of the Pacific plate as subduction inputs to the northeastern Japan arc and its implication for subduction zone processes"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Abstract</jats:title><jats:p>Devastating megathrust earthquakes and slow earthquakes both occur along subducting plate interfaces. These interplate seismic activities are strongly dependent on the nature of the plate interface, such as the shape of the plate interface and the materials and physical conditions along the plate interface. The oceanic plate, which is the input to the subduction zone, is the first order control on the nature of the plate interface. To reveal the nature of the subduction inputs to the northeastern Japan arc, we have conducted large-scale controlled-source seismic surveys of the northwestern part of the oceanic Pacific plate. The obtained seismic data have revealed (1) oceanic plate structural evolution caused by plate bending prior to subduction, suggesting the promotion of the oceanic plate hydration; (2) spatial variation of the oceanic plate structure, such as variations in the thickness of sediment and crust; (3) that the spatial variations are caused by both ancient plate formation processes and more recent volcanic activities; and (4) that spatial variations of the nature of the subduction inputs show good correlation with the along-strike variations in the seismic structure and seismic activities after subduction, including the coseismic slip distribution of the 2011 Tohoku earthquakes and the structural differences between the northern and the southern Japan Trench. These observations indicate that the incoming oceanic plate structure is much more spatially variable than previously thought and also imply that the spatial variation of the subduction inputs is a key controlling factor of the spatial variation of various processes in subduction zones, including interplate seismic activities and evolution of the forearc structure.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380021390563077512","@type":"Researcher","foaf:name":[{"@value":"Gou Fujie"}]},{"@id":"https://cir.nii.ac.jp/crid/1380021390563077652","@type":"Researcher","foaf:name":[{"@value":"Shuichi Kodaira"}]},{"@id":"https://cir.nii.ac.jp/crid/1380021390563077256","@type":"Researcher","foaf:name":[{"@value":"Koichiro Obana"}]},{"@id":"https://cir.nii.ac.jp/crid/1380021390563077538","@type":"Researcher","foaf:name":[{"@value":"Yojiro Yamamoto"}]},{"@id":"https://cir.nii.ac.jp/crid/1380021390563077249","@type":"Researcher","foaf:name":[{"@value":"Takehi Isse"}]},{"@id":"https://cir.nii.ac.jp/crid/1380021390563077505","@type":"Researcher","foaf:name":[{"@value":"Tomoaki Yamada"}]},{"@id":"https://cir.nii.ac.jp/crid/1380021390563077514","@type":"Researcher","foaf:name":[{"@value":"Tetsuo No"}]},{"@id":"https://cir.nii.ac.jp/crid/1380021390563077634","@type":"Researcher","foaf:name":[{"@value":"Yasuyuki Nakamura"}]},{"@id":"https://cir.nii.ac.jp/crid/1380021390563077122","@type":"Researcher","foaf:name":[{"@value":"Seiichi Miura"}]}],"publication":{"publicationIdentifier":[{"@type":"EISSN","@value":"21974284"}],"prism:publicationName":[{"@value":"Progress in Earth and Planetary Science"}],"dc:publisher":[{"@value":"Springer Science and Business Media LLC"}],"prism:publicationDate":"2023-08-22","prism:volume":"10","prism:number":"1","prism:startingPage":"1"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","dc:rights":["https://creativecommons.org/licenses/by/4.0","https://creativecommons.org/licenses/by/4.0"],"url":[{"@id":"https://link.springer.com/content/pdf/10.1186/s40645-023-00578-8.pdf"},{"@id":"https://link.springer.com/article/10.1186/s40645-023-00578-8/fulltext.html"}],"createdAt":"2023-08-22","modifiedAt":"2023-12-19","foaf:topic":[{"@id":"https://cir.nii.ac.jp/all?q=Controlled-source%20seismic%20survey","dc:title":"Controlled-source seismic survey"},{"@id":"https://cir.nii.ac.jp/all?q=G","dc:title":"G"},{"@id":"https://cir.nii.ac.jp/all?q=QE1-996.5","dc:title":"QE1-996.5"},{"@id":"https://cir.nii.ac.jp/all?q=Tohoku%20earthquake","dc:title":"Tohoku earthquake"},{"@id":"https://cir.nii.ac.jp/all?q=Japan%20Trench","dc:title":"Japan Trench"},{"@id":"https://cir.nii.ac.jp/all?q=Geography.%20Anthropology.%20Recreation","dc:title":"Geography. Anthropology. Recreation"},{"@id":"https://cir.nii.ac.jp/all?q=Oceanic%20crust","dc:title":"Oceanic crust"},{"@id":"https://cir.nii.ac.jp/all?q=Incoming%20oceanic%20plate","dc:title":"Incoming oceanic plate"},{"@id":"https://cir.nii.ac.jp/all?q=Geology","dc:title":"Geology"},{"@id":"https://cir.nii.ac.jp/all?q=Outer%20rise","dc:title":"Outer rise"}],"project":[{"@id":"https://cir.nii.ac.jp/crid/1040291932564658176","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"22H00167"},{"@type":"JGN","@value":"JP22H00167"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-22H00167/"}],"notation":[{"@language":"ja","@value":"アウターライズで海洋とマントルを結ぶ大規模流体循環の時空間スケールの解明"},{"@language":"en","@value":"Spatiotemporal scale of large-scale hydrothermal circulation system connecting ocean and mantle at the outer rise"}]},{"@id":"https://cir.nii.ac.jp/crid/1040295802078230144","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"23H00138"},{"@type":"JGN","@value":"JP23H00138"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-23H00138/"}],"notation":[{"@language":"ja","@value":"海洋アセノスフェアの粘性率を制約するための海底物理観測・モデリング国際協働研究"},{"@language":"en","@value":"International collaborative research on the viscosity of the oceanic asthenosphere through marine geophysical observations and geodynamic modeling"}]},{"@id":"https://cir.nii.ac.jp/crid/1040566775626660096","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"19H05596"},{"@type":"JGN","@value":"JP19H05596"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-19H05596/"}],"notation":[{"@language":"ja","@value":"巨大地震の裏側～巨大化させないメカニズム"},{"@language":"en","@value":"Head and tail of massive earthquakes: Mechanism arresting growth of interpolate earthquakes"}]}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050001339107234432","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Connecting slow earthquakes to huge earthquakes"},{"@value":"Connecting slow earthquakes to large earthquakes"}]},{"@id":"https://cir.nii.ac.jp/crid/1050013474495795840","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"A review on slow earthquakes in the Japan Trench"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002216709622528","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Systematic changes in the incoming plate structure at the Kuril trench"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002216807224192","@type":"Article","resourceType":"学術雑誌論文(journal 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double-planed shallow seismic zone in the NE Japan forearc region revealed by sP depth phases recorded by regional networks"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574095979827712","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Fault plane geometry in the source region of the 1994 Sanriku-oki earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574096506782976","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Structural characteristics controlling the seismicity crustal structure of southern Japan Trench fore-arc region, revealed by ocean bottom seismographic data"}]},{"@id":"https://cir.nii.ac.jp/crid/1360576120151965056","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A Global Data Set of Present‐Day Oceanic Crustal Age and Seafloor Spreading Parameters"}]},{"@id":"https://cir.nii.ac.jp/crid/1360584339765117952","@type":"Article","resourceType":"学術雑誌論文(journal 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