{"@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/1360848660458097664.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1111/iar.12121"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fiar.12121"}},{"identifier":{"@type":"URI","@value":"https://onlinelibrary.wiley.com/doi/pdf/10.1111/iar.12121"}}],"resourceType":"学術雑誌論文(journal article)","dc:title":[{"@value":"Fission track and U–Pb zircon ages of psammitic rocks from the Harushinai unit, Kamuikotan metamorphic rocks, central Hokkaido, Japan: constraints on metamorphic histories"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Abstract</jats:title><jats:p>Accurate pressure–temperature–time (<jats:italic>P–T–t</jats:italic>) paths of rocks from sedimentation through maximum burial to exhumation are needed to determine the processes and mechanisms that form high‐pressure and low‐temperature type metamorphic rocks. Here, we present a new method combining laser ablation–inductively coupled plasma–mass spectrometry (LA–ICP–MS) U–Pb with fission track (FT) dates for detrital zircons from two psammitic rock samples collected from the Harushinai unit of the Kamuikotan metamorphic rocks. The concordant zircon U–Pb ages for these samples vary markedly, from 1980 to 95 Ma, with the youngest age clusters in both samples yielding Albian‐Cenomanian weighted mean ages of 100.8 ± 1.1 and 99.3 ± 1.0 Ma (2σ uncertainties). The zircon U–Pb ages were not reset by high‐<jats:italic>P/T</jats:italic> type metamorphism, because there is no indication of overgrowth within the zircons with igneous oscillatory zoning. Therefore, these weighted mean ages are indicative of the maximum age of deposition of protolithic material. By comparison, the zircon FT data yield a pooled age of <jats:italic>ca.</jats:italic> 90 Ma, which is almost the same as the weighted mean age of the youngest U–Pb age cluster. This indicates that the zircon FT ages were reset at <jats:italic>ca.</jats:italic> 90 Ma while still at their source, but have not been reset since. This conclusion is supported by recorded temperature conditions of less than about 300 °C (the closure temperature of zircon FTs), as estimated from microstructures in the deformed detrital quartz grains in psammitic rocks, and no shortening of fission track lengths in the zircon. Combining these new data with previously reported white mica K–Ar ages indicates that the Harushinai unit was deposited after <jats:italic>ca.</jats:italic> 100 Ma, and underwent burial to its maximum depth before being subjected to a localized thermal overprint during exhumation at <jats:italic>ca.</jats:italic> 58 Ma.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380848660458097806","@type":"Researcher","foaf:name":[{"@value":"Ayumi S. Okamoto"}],"jpcoar:affiliationName":[{"@value":"Department of Natural History Sciences, Graduate School of Sciences Hokkaido University  Sapporo 060‐0810 Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380848660458097935","@type":"Researcher","foaf:name":[{"@value":"Toru Takeshita"}],"jpcoar:affiliationName":[{"@value":"Department of Natural History Sciences, Graduate School of Sciences Hokkaido University  Sapporo 060‐0810 Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380848660458097675","@type":"Researcher","foaf:name":[{"@value":"Hideki Iwano"}],"jpcoar:affiliationName":[{"@value":"Kyoto Fission‐Track Co., Ltd.  Kita Kyoto 603‐8832 Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380848660458097543","@type":"Researcher","foaf:name":[{"@value":"Tohru Danhara"}],"jpcoar:affiliationName":[{"@value":"Kyoto Fission‐Track Co., Ltd.  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Hirata"}],"jpcoar:affiliationName":[{"@value":"Division of Earth and Planetary Sciences Kyoto University  Sakyo Kyoto 606‐8502 Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380848660458097797","@type":"Researcher","foaf:name":[{"@value":"Hirotsugu Nishido"}],"jpcoar:affiliationName":[{"@value":"Okayama University of Science  1‐1 Ridai‐cho, Kita‐ku Okayama 700‐0005 Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380848660458097547","@type":"Researcher","foaf:name":[{"@value":"Shuhei Sakata"}],"jpcoar:affiliationName":[{"@value":"Division of Earth and Planetary Sciences Kyoto University  Sakyo Kyoto 606‐8502 Japan"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"10384871"},{"@type":"EISSN","@value":"14401738"}],"prism:publicationName":[{"@value":"Island Arc"}],"dc:publisher":[{"@value":"Wiley"}],"prism:publicationDate":"2015-11-27","prism:volume":"24","prism:number":"4","prism:startingPage":"379","prism:endingPage":"403"},"reviewed":"false","invited":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fiar.12121"},{"@id":"https://onlinelibrary.wiley.com/doi/pdf/10.1111/iar.12121"}],"createdAt":"2015-11-27","modifiedAt":"2023-10-03","project":[{"@id":"https://cir.nii.ac.jp/crid/1040282257255938944","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"26109004"},{"@type":"JGN","@value":"JP26109004"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PLANNED-26109004/"}],"notation":[{"@language":"ja","@value":"観察・観測による断層帯の発達過程とミクロからマクロまでの地殻構造の解明"},{"@language":"en","@value":"Investigation of fault development and crustal structure from microscopic to macroscopic scales based on geological and seismic observations"}]},{"@id":"https://cir.nii.ac.jp/crid/1040282257413729408","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"13J03294"},{"@type":"JGN","@value":"JP13J03294"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-13J03294/"}],"notation":[{"@language":"ja","@value":"岩石の微細構造観察と変形実験に基づくプレート沈み込み帯の動力学の解明"}]}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050025031480436224","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Coupled micro-faulting and pressure solution creep overprinted on quartz schist deformed by intracrystalline plasticity during exhumation of the Sambagawa metamorphic rocks, southwest Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002218164275712","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"An inter‐laboratory evaluation of <scp>OD</scp>‐3 zircon for 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