{"@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/1361137045269564288.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1007/bf00287112"}},{"identifier":{"@type":"URI","@value":"http://link.springer.com/content/pdf/10.1007/BF00287112.pdf"}},{"identifier":{"@type":"URI","@value":"http://link.springer.com/article/10.1007/BF00287112/fulltext.html"}},{"identifier":{"@type":"URI","@value":"http://link.springer.com/content/pdf/10.1007/BF00287112"}},{"identifier":{"@type":"DOI","@value":"10.1007/s004100050065"}},{"identifier":{"@type":"NAID","@value":"80008389394"}}],"dc:title":[{"@value":"Timing of the cataclastic deformation along the Akaishi Tectonic Line, central Japan"}],"description":[{"notation":[{"@value":"This paper describes K-Ar ages of cataclasites and fault gouges from the Akaishi Tectonic Line (ATL), central Japan. Petrological and mineralogical features of these rocks are also examined. Based on the results, we test the hypothesis that the K-Ar ages of these rocks represent the age of hydrothermal alteration associated with the fault movement. Intensity of deformation and alteration increase passing from host rock into cataclasite and finally into fault gouge. This increase corresponds to an increase of the value of crystallinity index (Kubler index) of the micaceous minerals contained in these rocks. Furthermore, the degree of rejuvention of K-Ar ages of the micaceous minerals increases in the same sense. A correlation of K-Ar ages (plotted on the y axis) versus Kubler index (plotted on the x axis) yields a concave curve asymptotically parallel with the x axis at approximately 15 Ma. This curve is interpreted to represent the mode of decrease of the relative amounts of inherited argon in the K-Ar system of the micaceous minerals, corresponding to an increase in the intensity of deformation and alteration. Inclination of the curve becomes zero if all the inherited argon is lost from the K-Ar system of the micaceous minerals. Thus, it is concluded that the hydrothermal alteration occurred at approximately 15 Ma. The strike-slip basin along the ATL formed the middle Miocene. The K-Ar dating of ATL gouges indicates that the ATL was active simultaneously with formation of the strike-slip basin along its trace during the middle Miocene."}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1381137045269564289","@type":"Researcher","foaf:name":[{"@value":"Hidemi Tanaka"}]},{"@id":"https://cir.nii.ac.jp/crid/1381137045269564160","@type":"Researcher","foaf:name":[{"@value":"Nobuo Uehara"}]},{"@id":"https://cir.nii.ac.jp/crid/1381137045269564288","@type":"Researcher","foaf:name":[{"@value":"Tetsumaru Itaya"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00107999"},{"@type":"EISSN","@value":"14320967"}],"prism:publicationName":[{"@value":"Contributions to Mineralogy and Petrology"}],"dc:publisher":[{"@value":"Springer Science and Business Media LLC"}],"prism:publicationDate":"1995-06","prism:volume":"120","prism:number":"2","prism:startingPage":"150","prism:endingPage":"158"},"reviewed":"false","dc:rights":["http://www.springer.com/tdm"],"url":[{"@id":"http://link.springer.com/content/pdf/10.1007/BF00287112.pdf"},{"@id":"http://link.springer.com/article/10.1007/BF00287112/fulltext.html"},{"@id":"http://link.springer.com/content/pdf/10.1007/BF00287112"}],"createdAt":"2004-10-30","modifiedAt":"2019-04-08","foaf:topic":[{"@id":"https://cir.nii.ac.jp/all?q=Geochemistry%20and%20Petrology","dc:title":"Geochemistry and Petrology"},{"@id":"https://cir.nii.ac.jp/all?q=Geophysics","dc:title":"Geophysics"}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050282810708740608","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Thermochronological investigation of fault 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problems"}]},{"@id":"https://cir.nii.ac.jp/crid/1570854175591554176","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Distribution of fault rocks in the fracture zone of the Nojima Fault at a depth of 1140m : Observations from the Hirabayashi NIED drill core"}]},{"@id":"https://cir.nii.ac.jp/crid/1574231875312459776","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Shuffled-cards structure and different P/T conditions in the Sanbagawa metamorphic belt, Sakuma-Tenryu area, central Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/2051714792046940032","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Changes in illite crystallinity within an ancient tectonic boundary thrust caused by thermal, mechanical, and hydrothermal effects : an example from the Nobeoka Thrust, southwest 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