{"@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/1361137043692926464.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1130/0091-7613(1997)025<0327:psotsa>2.3.co;2"}}],"dc:title":[{"@value":"Paleothermal structure of the Shimanto accretionary prism, Shikoku, Japan: Role of an out-of-sequence thrust"}],"description":[{"notation":[{"@value":"Vitrinite reflectance study on the Cretaceous Shimanto accretionary prism of Southwest Japan shows that the vitrinite reflectance varies from 0.6% to 3.0%, corresponding to the estimated maximum paleotemperature variation of 90–210 °C. The thermal structure shows a sharp discontinuity across an out-of-sequence thrust separating it into two thermal blocks. In each block, vitrinite reflectance values increase systematically toward the prism younging direction, and the thermal structure is clearly overprinted on the tectonic imbrication of turbidite and melange units. This provided us with a set of data to calculate the geometry and displacement of the out-of-sequence thrust. The fission-track zircon partial-annealing ages indicate that this thrust was active about 43 Ma, probably in response to the accretion of Eocene rocks. This study shows that initial thickening of the accretionary prism, in an order of several kilometres, was mainly controlled by out-of-sequence thrust."}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1381137043692926467","@type":"Researcher","foaf:name":[{"@value":"Kotoe Ohmori"}]},{"@id":"https://cir.nii.ac.jp/crid/1381137043692926469","@type":"Researcher","foaf:name":[{"@value":"Asahiko Taira"}]},{"@id":"https://cir.nii.ac.jp/crid/1381137043692926466","@type":"Researcher","foaf:name":[{"@value":"Hidekazu Tokuyama"}]},{"@id":"https://cir.nii.ac.jp/crid/1381137043692926464","@type":"Researcher","foaf:name":[{"@value":"Arito Sakaguchi"}]},{"@id":"https://cir.nii.ac.jp/crid/1381137043692926465","@type":"Researcher","foaf:name":[{"@value":"Makoto Okamura"}]},{"@id":"https://cir.nii.ac.jp/crid/1381137043692926468","@type":"Researcher","foaf:name":[{"@value":"Atsuo Aihara"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00917613"}],"prism:publicationName":[{"@value":"Geology"}],"dc:publisher":[{"@value":"Geological Society of America"}],"prism:publicationDate":"1997","prism:volume":"25","prism:number":"4","prism:startingPage":"327"},"reviewed":"false","createdAt":"2002-07-27","modifiedAt":"2018-03-08","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050011340342223872","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Evidence of Localized Failure Along Altered Basaltic Blocks in Tectonic Mélange at the Updip Limit of the Seismogenic Zone: Implications for the Shallow Slow Earthquake Source"}]},{"@id":"https://cir.nii.ac.jp/crid/1050306506454155648","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Alteration and dehydration of 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Japan."},{"@language":"ja","@value":"徳島県南東部に分布する四万十帯玄武岩類の変質作用"},{"@language":"ja-Kana","@value":"トクシマケン ナントウブ ニ ブンプ スル シマントタイ ゲンブガンルイ ノ ヘンシツ サヨウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681215696256","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Evaluation of the displacement of the Tsugaru Fault by means of organic maturity of fossil pollen in sediments"},{"@language":"ja","@value":"化石花粉の有機熟成度から津軽断層の変位量を推定する"},{"@language":"ja-Kana","@value":"カセキ カフン ノ ユウキ ジュクセイド カラ ツガル ダンソウ ノ ヘンイリョウ オ スイテイ スル"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681217746048","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Deformation and fluid flow in seismogenic subduction zone: The Mugi Mélange in the Shimanto Belt"},{"@language":"ja","@value":"四万十帯牟岐メランジュにみる沈み込み帯地震発生帯の変形と流体移動"}]},{"@id":"https://cir.nii.ac.jp/crid/1390287474423766656","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Deformation structures in the tectonic mélange of the Jurassic Chizu Complex, Okayama Prefecture, Southwest Japan"},{"@language":"ja","@value":"ジュラ系智頭コンプレックス中にみられるテクトニック・メランジュの変形構造"},{"@language":"ja-Kana","@value":"ジュラケイチトウ コンプレックス チュウ ニ ミラレル テクトニック ・ メランジュ ノ ヘンケイ コウゾウ"}]},{"@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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