{"@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/1360004232324926976.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1016/j.jsg.2013.03.015"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0191814113000552?httpAccept=text/xml"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0191814113000552?httpAccept=text/plain"}}],"resourceType":"学術雑誌論文(journal article)","dc:title":[{"@value":"Hanging wall deformation of a seismogenic megasplay fault in an accretionary prism: The Nobeoka Thrust in southwestern Japan"}],"description":[{"notation":[{"@value":"The structure and occurrence of deformation within the hanging wall of the Nobeoka Thrust in Kyushu, Japan, was investigated to understand the dynamic aspects of splay faulting in relation to seismic events. From field observations, hanging wall is suggested to have undergone four phases of deformation. The first phase involved horizontal shortening, as documented by folding and thrusting, followed by a phase of vertical loading shown by the development of horizontal slaty cleavages, pressure solution, and cleavage-parallel mineral vein precipitation. A third phase involved shearing, and deformation along cleavage restricted to near the Nobeoka Thrust, while the fourth phase produced widespread, brittle fracturing associated with the development of pseudotachylyte-bearing faults and tension crack filling veins high angle to cleavage. These four phases can be explained as follows. During the inter-seismic period, an extensionally stable taper was maintained in the inner wedge of the accretionary prism by dominant vertical loading (σ1), in combination with a lesser amount of horizontal compression (σ2) related to the locking of the mega-thrust. Elastic strain energy in the hanging wall of the inner wedge was co-seismically released by slip on the mega-thrust and horizontal shortening in the outer wedge associated with dynamic ductile weakening of the fault plane. This sudden release of elastic strain caused brittle fracturing with σ1 at a high angle to the shear surface of the Nobeoka Thrust, most of the displacement resulting from deformation of the footwall."}]},{"notation":[{"@value":"International 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(JAMSTEC)"}]},{"@id":"https://cir.nii.ac.jp/crid/1892553967674885512","@type":"Researcher","foaf:name":[{"@value":"Institut des Sciences de la Terre d'Orléans - UMR7327 (ISTO) ; Bureau de Recherches Géologiques et Minières (BRGM)-Observatoire des Sciences de l'Univers en région Centre (OSUC) ; Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire de Paris ; Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-Université d'Orléans (UO)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire de Paris ; Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-Université d'Orléans (UO)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Université d'Orléans (UO)-Centre National de la Recherche Scientifique (CNRS)"}]},{"@id":"https://cir.nii.ac.jp/crid/1892553967674885506","@type":"Researcher","foaf:name":[{"@value":"Institut des Sciences de la Terre d'Orléans - UMR7327 (ISTO) ; Bureau de Recherches Géologiques et Minières (BRGM) (BRGM)-Observatoire des Sciences de l'Univers en région Centre (OSUC) ; Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire de Paris ; Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université d'Orléans (UO)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire de Paris ; Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université d'Orléans (UO)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Université d'Orléans (UO)-Centre National de la Recherche Scientifique (CNRS)"}]},{"@id":"https://cir.nii.ac.jp/crid/1892553967674885508","@type":"Researcher","foaf:name":[{"@value":"Institut des Sciences de la Terre d'Orléans - UMR7327 (ISTO) ; Centre National de la Recherche Scientifique (CNRS)-Université d'Orléans (UO)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire des Sciences de l'Univers en région Centre (OSUC) ; Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université d'Orléans (UO)-Observatoire de Paris ; Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université d'Orléans (UO)-Observatoire de Paris ; Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Bureau de Recherches Géologiques et Minières (BRGM) (BRGM)"}]},{"@id":"https://cir.nii.ac.jp/crid/1892555065823238404","@type":"Researcher","foaf:name":[{"@value":"POTHIER, Nathalie"}]},{"@id":"https://cir.nii.ac.jp/crid/1892555065823238405","@type":"Researcher","foaf:name":[{"@value":"Graduate School of Science Tokyo"}]},{"@id":"https://cir.nii.ac.jp/crid/1892555065823238409","@type":"Researcher","foaf:name":[{"@value":"Department of Earth and Planetary Science Tokyo"}]},{"@id":"https://cir.nii.ac.jp/crid/1892555065823238400","@type":"Researcher","foaf:name":[{"@value":"The University of Tokyo (UTokyo)-The University of Tokyo (UTokyo)"}]},{"@id":"https://cir.nii.ac.jp/crid/1892555065823238410","@type":"Researcher","foaf:name":[{"@value":"Japan Agency for Marine-Earth Science and Technology (JAMSTEC)"}]},{"@id":"https://cir.nii.ac.jp/crid/1892555065823238401","@type":"Researcher","foaf:name":[{"@value":"Institute for Research on Earth Evolution Yokosuka (IFREE)"}]},{"@id":"https://cir.nii.ac.jp/crid/1892555065823238402","@type":"Researcher","foaf:name":[{"@value":"Institut des Sciences de la Terre d'Orléans - UMR7327 (ISTO)"}]},{"@id":"https://cir.nii.ac.jp/crid/1892555065823238407","@type":"Researcher","foaf:name":[{"@value":"Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire de Paris"}]},{"@id":"https://cir.nii.ac.jp/crid/1892555065823238406","@type":"Researcher","foaf:name":[{"@value":"Bureau de Recherches Géologiques et Minières (BRGM) (BRGM)-Observatoire des Sciences de l'Univers en région Centre (OSUC)"}]},{"@id":"https://cir.nii.ac.jp/crid/1892555065823238403","@type":"Researcher","foaf:name":[{"@value":"Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université d'Orléans (UO)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Université d'Orléans (UO)-Centre National de la Recherche Scientifique (CNRS)"}]},{"@id":"https://cir.nii.ac.jp/crid/1892555065823238408","@type":"Researcher","foaf:name":[{"@value":"Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université d'Orléans (UO)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire de Paris"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"01918141"}],"prism:publicationName":[{"@value":"Journal of Structural Geology"}],"dc:publisher":[{"@value":"Elsevier BV"}],"prism:publicationDate":"2013-07","prism:volume":"52","prism:startingPage":"136","prism:endingPage":"147"},"reviewed":"false","dc:rights":["https://www.elsevier.com/tdm/userlicense/1.0/"],"url":[{"@id":"https://api.elsevier.com/content/article/PII:S0191814113000552?httpAccept=text/xml"},{"@id":"https://api.elsevier.com/content/article/PII:S0191814113000552?httpAccept=text/plain"}],"createdAt":"2013-04-16","modifiedAt":"2019-07-12","foaf:topic":[{"@id":"https://cir.nii.ac.jp/all?q=%5BSDU.STU.TE%5DSciences%20of%20the%20Universe%20%5Bphysics%5D/Earth%20Sciences/Tectonics","dc:title":"[SDU.STU.TE]Sciences of the Universe [physics]/Earth Sciences/Tectonics"},{"@id":"https://cir.nii.ac.jp/all?q=%5BSDE.MCG%5D%20Environmental%20Sciences/Global%20Changes","dc:title":"[SDE.MCG] Environmental Sciences/Global Changes"},{"@id":"https://cir.nii.ac.jp/all?q=Subduction%20zone","dc:title":"Subduction zone"},{"@id":"https://cir.nii.ac.jp/all?q=550","dc:title":"550"},{"@id":"https://cir.nii.ac.jp/all?q=Megasplay%20fault","dc:title":"Megasplay fault"},{"@id":"https://cir.nii.ac.jp/all?q=Accretionary%20prism","dc:title":"Accretionary prism"},{"@id":"https://cir.nii.ac.jp/all?q=%5BSDE.MCG%5DEnvironmental%20Sciences/Global%20Changes","dc:title":"[SDE.MCG]Environmental Sciences/Global Changes"},{"@id":"https://cir.nii.ac.jp/all?q=%5BSDU.STU.TE%5D%20Sciences%20of%20the%20Universe%20%5Bphysics%5D/Earth%20Sciences/Tectonics","dc:title":"[SDU.STU.TE] Sciences of the Universe [physics]/Earth Sciences/Tectonics"},{"@id":"https://cir.nii.ac.jp/all?q=Stress%20orientation","dc:title":"Stress orientation"}],"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 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