{"@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/1361699993805333376.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/2004tc001655"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2004TC001655"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2004TC001655"}}],"dc:title":[{"@value":"Deformation and fluid flow of a major out‐of‐sequence thrust located at seismogenic depth in an accretionary complex: Nobeoka Thrust in the Shimanto Belt, Kyushu, Japan"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>Nobeoka Thrust in Kyushu, southwest Japan, was investigated to understand the relationship between the seismogenic out‐of‐sequence thrust (OST) and fluid flow in accretionary prisms. The Nobeoka Thrust is a fossilized OST, being active at seismogenic depth. The hanging wall exhibits a penetrative plastic deformation, while a brittle, cataclastic mélange‐like occurrence characterizes the footwall, although both of them have same shale and sandstone‐dominant protolith. Vitrinite reflectance analyses indicate that the maximum temperatures of the hanging wall and footwall are approximately 320 and 250°C, respectively. This thermal gap across the thrust corresponds to 8.6–14.4 km of displacement assuming a 28–47°C/km geothermal gradient. The brittle damage zone of the thrust is asymmetric: only 2 m for hanging wall side and 100 m for footwall. Three types of mineral veins, quartz, and carbonate are well developed, especially in the damaged footwall: the tension crack‐filling vein, the fault‐filling vein, and postmélange one. The first is harmonious with fabric, perpendicular to the <jats:italic>P</jats:italic> surface. Fluid inclusion geothermobarometry indicates the <jats:italic>P</jats:italic>‐<jats:italic>T</jats:italic> of fluid in the intensively damaged zone of the footwall is ∼300°C, 230–250 MPa, higher than that from vitrinite reflectance, which suggests that hydrothermal fluid flow is associated with deformation. The same type vein in the lowest portion of the footwall‐damaged zone includes a much lower <jats:italic>P</jats:italic>‐<jats:italic>T</jats:italic> fluid. This difference suggests that continuous underplating caused the damaged zone to propagate downward with cooling and shallowing, which differs from faults characterized by shear localization and might be unique to aquiferous OST in accretionary complexes.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1381699993805333381","@type":"Researcher","foaf:name":[{"@value":"Hideki Kondo"}],"jpcoar:affiliationName":[{"@value":"Department of Earth and Planetary Sciences University of Tokyo  Tokyo Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1381699993805333383","@type":"Researcher","foaf:name":[{"@value":"Gaku Kimura"}],"jpcoar:affiliationName":[{"@value":"Department of Earth and Planetary Sciences University of Tokyo  Tokyo Japan"},{"@value":"Institute for Research on Earth Evolution Japan Agency for Marine‐Earth Science and Technology  Yokohama Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1381699993805333376","@type":"Researcher","foaf:name":[{"@value":"Hideki Masago"}],"jpcoar:affiliationName":[{"@value":"Center for Deep Earth Exploration Japan Agency for Marine‐Earth Science and Technology  Yokohama Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380861294510311040","@type":"Researcher","foaf:name":[{"@value":"Kotoe Ohmori‐Ikehara"}],"jpcoar:affiliationName":[{"@value":"Department of Natural Environmental Science Kochi University  Kochi Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1381699993805333377","@type":"Researcher","foaf:name":[{"@value":"Yujin Kitamura"}],"jpcoar:affiliationName":[{"@value":"Department of Earth and Planetary Sciences University of Tokyo  Tokyo Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1381699993805333379","@type":"Researcher","foaf:name":[{"@value":"Eisei Ikesawa"}],"jpcoar:affiliationName":[{"@value":"Department of Earth and Planetary Sciences University of Tokyo  Tokyo Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1381699993805333380","@type":"Researcher","foaf:name":[{"@value":"Arito Sakaguchi"}],"jpcoar:affiliationName":[{"@value":"Institute for Research on Earth Evolution Japan Agency for Marine‐Earth Science and Technology  Yokohama Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1381699993805333382","@type":"Researcher","foaf:name":[{"@value":"Asuka Yamaguchi"}],"jpcoar:affiliationName":[{"@value":"Department of Earth and Planetary Sciences University of Tokyo  Tokyo Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1381699993805333378","@type":"Researcher","foaf:name":[{"@value":"Shin'ya Okamoto"}],"jpcoar:affiliationName":[{"@value":"Department of Earth and Planetary Sciences University of Tokyo  Tokyo Japan"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"02787407"},{"@type":"EISSN","@value":"19449194"}],"prism:publicationName":[{"@value":"Tectonics"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"2005-11-23","prism:volume":"24","prism:number":"6","prism:startingPage":"1"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2004TC001655"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2004TC001655"}],"createdAt":"2005-11-22","modifiedAt":"2023-10-12","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050855765273939328","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Deformation Structures From Splay and Décollement Faults in the Nankai Accretionary Prism, SW Japan(IODP NanTroSEIZE Expedition 316): Evidence for Slow and Rapid Slip in Fault Rocks"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002214351202688","@type":"Article","resourceType":"学術雑誌論文(journal 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Japan"},{"@language":"ja","@value":"紀州白亜系四万十帯美山層のメランジュ変形構造と温度圧力履歴"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681217126656","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"The relationship between displacement and thickness of faults in the Shimanto accretionary complex"},{"@language":"ja","@value":"付加体内部に発達する断層の変位量と幅との相関関係"},{"@language":"ja-Kana","@value":"フカ タイナイブ ニ ハッタツ スル ダンソウ ノ ヘンイリョウ ト ハバ ト ノ ソウカン カンケイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390568617217795584","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"On approximations of EASY%Ro solutions to estimate maximum temperature from vitrinite reflectance"},{"@value":"On approximations of EASY%R₀ solutions to estimate maximum temperature from vitrinite 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