{"@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/1390282681490834944.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1186/bf03353343"}},{"identifier":{"@type":"URI","@value":"https://link.springer.com/content/pdf/10.1186/BF03353343.pdf"}},{"identifier":{"@type":"URI","@value":"https://link.springer.com/article/10.1186/BF03353343/fulltext.html"}},{"identifier":{"@type":"URI","@value":"http://link.springer.com/content/pdf/10.1186/BF03353343"}},{"identifier":{"@type":"NAID","@value":"130003780997"}}],"dc:title":[{"@language":"en","@value":"Occurrence of mylonite zones and pseudotachylyte veins around the base of the upper crust"},{"@value":"Occurrence of mylonite zones and pseudotachylyte veins around the base of the upper crust: An example from the southern Hidaka metamorphic belt, Samani area, Hokkaido, Japan"}],"dcterms:alternative":[{"@language":"en","@value":"An example from the southern Hidaka metamorphic belt, Samani area, Hokkaido, Japan"}],"dc:language":"en","description":[{"type":"abstract","notation":[{"@language":"en","@value":"Geological studies on exhumed pseudotachylyte-bearing mylonite zones in S-type tonalite were carried out in the southern Hidaka metamorphic belt, Hokkaido, Japan. Mylonitization is characterized by (1) development of composite planar fabrics, (2) grain size reduction, and (3) change in modal composition an increase in mica content and a decrease in quartz content from protolith to mylonite. Mylonite zones are heterogeneously concentrated in the host rocks. At microscopic scales, shear deformation is concentrated heterogeneously in finegrained layers along C-surfaces. Most of the pseudotachylyte layers are subparallel to the C-surface, and tend to overprint thick mylonite zones. The heterogeneous development of mylonite zones, which may be activated as layers of co-seismic slip, should be incorporated into numerical modeling of seismogenic zones."}],"abstractLicenseFlag":"disallow"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1410282681490834945","@type":"Researcher","personIdentifier":[{"@type":"NRID","@value":"9000254262925"}],"foaf:name":[{"@language":"en","@value":"Shimada Koji"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Department of Earth and Planetary Science, The University of Tokyo"}]},{"@id":"https://cir.nii.ac.jp/crid/1410282681490834947","@type":"Researcher","personIdentifier":[{"@type":"NRID","@value":"9000254262926"}],"foaf:name":[{"@language":"en","@value":"Tanaka Hidemi"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Department of Earth and Planetary Science, The University of 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日本火山学会、日本測地学会、日本惑星科学会"}],"prism:publicationDate":"2004","prism:volume":"56","prism:number":"12","prism:startingPage":"1217","prism:endingPage":"1223"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","url":[{"@id":"https://link.springer.com/content/pdf/10.1186/BF03353343.pdf"},{"@id":"https://link.springer.com/article/10.1186/BF03353343/fulltext.html"},{"@id":"http://link.springer.com/content/pdf/10.1186/BF03353343"}],"availableAt":"2004","foaf:topic":[{"@id":"https://cir.nii.ac.jp/all?q=Pseudotachylyte","dc:title":"Pseudotachylyte"},{"@id":"https://cir.nii.ac.jp/all?q=mylonite","dc:title":"mylonite"},{"@id":"https://cir.nii.ac.jp/all?q=strain%20localization","dc:title":"strain localization"},{"@id":"https://cir.nii.ac.jp/all?q=Hidaka%20metamorphic%20belt","dc:title":"Hidaka metamorphic 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Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681215581184","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Metamorphic and deformation processes of lower crustal rocks in the Hidaka CollisionZone, Hokkaido, northern Japan"},{"@language":"ja","@value":"日高衝突帯下部地殻の岩石構成と変形運動"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681490857344","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Heterogeneous material distribution, an important reason for generation of strain-localized mylonite and frictional slip zones in the Hidaka metamorphic belt, Hokkaido, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1390564238052793472","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Architecture of onshore fault zones"},{"@language":"ja","@value":"陸域断層の内部構造"},{"@language":"ja-Kana","@value":"リクイキ ダンソウ ノ 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