{"@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/1363388844879716480.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1016/j.jseaes.2008.11.015"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S136791200800196X?httpAccept=text/xml"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S136791200800196X?httpAccept=text/plain"}}],"dc:title":[{"@value":"Mid-crustal horizontal shear zone in the forearc region of the mid-Cretaceous SW Japan arc, inferred from strain analysis of rocks within the Ryoke metamorphic belt"}],"description":[{"notation":[{"@value":"Abstract   The strain geometry of a Cretaceous low- P /high- T  metamorphosed accretionary complex in SW Japan is one of the key geological constraints in understanding the Cretaceous tectonics of the forearc region at the eastern margin of Eurasia. We studied the strain geometry of upper greenschist to lower amphibolite facies metamorphic rocks from the mid-Cretaceous low- P /high- T  Ryoke metamorphic belt, which during the mid-Cretaceous were located at mid-crustal depths close to the volcanic front. Strain analysis focused on deformed radiolarian fossils in metachert and sandstone/chert clasts within metapelite. The maximum stretching direction ( X -direction) of the strain ellipsoid of the schistosity-forming deformation at the peak metamorphism is oriented E-W, and the  XY -plane of the strain ellipsoid developed parallel to schistosity. The metachert and metapelite exhibit plane strain to general flattening strain that probably largely resulted from the schistosity-forming deformation. Based on the results of the previous strain analyses and this study, it reveals that the schistosity-forming deformation occurred under bedding-normal shortening, resulting in general flattening strain throughout the Ryoke metamorphic belt. The  X -direction of the strain ellipsoid of the schistosity-forming deformation is oriented parallel to the length of the Ryoke metamorphic belt throughout the SW Japan arc. The schistosity formed parallel to bedding planes that developed horizontally in non-metamorphosed accretionary complexes of SW Japan, indicating horizontal  XY -plane of the strain ellipsoid. These observations indicate the occurrence of horizontal shear deformation within the middle crust (∼15 km depth) at the time of the low- P /high- T  metamorphism. The deep-seated horizontal shear zone and the shallower incipient Median Tectonic Line (MTL) fault system could result in a crustal-scale detachment fault in the forearc region of the mid-Cretaceous SW Japan arc. After the formation of the detachment, the left-lateral pull-apart forearc basins, Onogawa-Izumi Group distributed on the north side of the MTL and the southern marginal mylonite zone might be formed by the sinistral movement along the detachment fault."}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1383388844879716481","@type":"Researcher","foaf:name":[{"@value":"Takamoto Okudaira"}]},{"@id":"https://cir.nii.ac.jp/crid/1383388844879716480","@type":"Researcher","foaf:name":[{"@value":"Yuki Beppu"}]},{"@id":"https://cir.nii.ac.jp/crid/1383388844879716482","@type":"Researcher","foaf:name":[{"@value":"Ryosuke Yano"}]},{"@id":"https://cir.nii.ac.jp/crid/1383388844879716483","@type":"Researcher","foaf:name":[{"@value":"Mio Tsuyama"}]},{"@id":"https://cir.nii.ac.jp/crid/1383388844879716484","@type":"Researcher","foaf:name":[{"@value":"Kazuhiko Ishii"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"13679120"}],"prism:publicationName":[{"@value":"Journal of Asian Earth Sciences"}],"dc:publisher":[{"@value":"Elsevier BV"}],"prism:publicationDate":"2009-06","prism:volume":"35","prism:number":"1","prism:startingPage":"34","prism:endingPage":"44"},"reviewed":"false","dc:rights":["https://www.elsevier.com/tdm/userlicense/1.0/","https://www.elsevier.com/legal/tdmrep-license"],"url":[{"@id":"https://api.elsevier.com/content/article/PII:S136791200800196X?httpAccept=text/xml"},{"@id":"https://api.elsevier.com/content/article/PII:S136791200800196X?httpAccept=text/plain"}],"createdAt":"2008-12-25","modifiedAt":"2025-10-24","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360002216709061888","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Estimates of stress and strain rate in mylonites based on the boundary between the fields of grain‐size sensitive and insensitive 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Southwest Japan: Provenance analysis of the Yuasa–Aridagawa basin based on U–Pb zircon ages"}]},{"@id":"https://cir.nii.ac.jp/crid/1360580230605692288","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Kinetics and pulses of zircon growth in migmatites beneath a volcanic arc: An example from the high‐<i>T</i> Ryoke Complex, southwest Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360584340704397568","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Paired Metamorphism of SW Japan and Implications for Tectonics of Convergent Margins"}]},{"@id":"https://cir.nii.ac.jp/crid/1360584340709577728","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Syn-tectonic development of the shape preferred orientation of phyllosilicates: A two-dimensional simulation of foliation 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