{"@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/1360285708268515840.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/2018gl080579"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2018GL080579"}},{"identifier":{"@type":"URI","@value":"https://onlinelibrary.wiley.com/doi/pdf/10.1029/2018GL080579"}},{"identifier":{"@type":"URI","@value":"https://onlinelibrary.wiley.com/doi/full-xml/10.1029/2018GL080579"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/am-pdf/10.1029/2018GL080579"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2018GL080579"}},{"identifier":{"@type":"HANDLE","@value":"20.500.11937/73990"}}],"resourceType":"学術雑誌論文(journal article)","dc:title":[{"@value":"Rapid Exhumation of Earth's Youngest Exposed Granites Driven by Subduction of an Oceanic Arc"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Abstract</jats:title><jats:p>Exhumation of plutonic systems is driven by a range of mechanisms including isostatic, tectonic, and erosional processes. Variable rates of plutonic exhumation in active subduction systems may be driven by idiosyncrasies of regional geology or by first‐order tectonic features. We report new age, isotope, and low‐temperature thermochronology constraints of granitoids from the Hida Mountains of central Japan that constrain the highest rates and magnitude of plutonic rock exhumation within the Japan and one of the highest worldwide. This extreme exhumation is centered on the apex of a lithospheric scale anticlinorium associated with the subduction of the Izu‐Bonin oceanic arc. The spatial and temporal relationship between the exhumation of these Pleistocene plutons and the subducting/accreting Izu‐Bonin oceanic arc links the plate‐scale geodynamics and regional exhumation patterns. Identifying thermochronological anomalies within magmatic arcs provides an opportunity to identify ancient asperities previously subducted and responsible for rapid exhumation rates within ancient subduction systems.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380013168760814098","@type":"Researcher","foaf:name":[{"@value":"C. J. Spencer"}],"jpcoar:affiliationName":[{"@value":"Earth Dynamics Research Group, The Institute of Geoscience Research, School of Earth and Planetary Sciences Curtin University  Perth Western Australia Australia"}]},{"@id":"https://cir.nii.ac.jp/crid/1380285708268515841","@type":"Researcher","foaf:name":[{"@value":"M. Danišík"}],"jpcoar:affiliationName":[{"@value":"John de Laeter Centre, The Institute of Geoscience Research Curtin University  Perth Western Australia Australia"}]},{"@id":"https://cir.nii.ac.jp/crid/1380285708268515971","@type":"Researcher","foaf:name":[{"@value":"H. Ito"}],"jpcoar:affiliationName":[{"@value":"Geosphere Science Sector Central Research Institute of Electric Power Industry  Chiba Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380285708268515968","@type":"Researcher","foaf:name":[{"@value":"C. Hoiland"}],"jpcoar:affiliationName":[{"@value":"Department of Geological Sciences Stanford University  Stanford CA USA"}]},{"@id":"https://cir.nii.ac.jp/crid/1380285708268515975","@type":"Researcher","foaf:name":[{"@value":"S. Tapster"}],"jpcoar:affiliationName":[{"@value":"NERC Isotope Geosciences Facilities British Geological Survey  Nottingham UK"}]},{"@id":"https://cir.nii.ac.jp/crid/1380285708268515970","@type":"Researcher","foaf:name":[{"@value":"H. Jeon"}],"jpcoar:affiliationName":[{"@value":"Centre for Microscopy, Characterisation and Analysis University of Western Australia  Perth Western Australia Australia"},{"@value":"Now at the Swedish Museum of Natural History  Stockholm Sweden"}]},{"@id":"https://cir.nii.ac.jp/crid/1380285708268515842","@type":"Researcher","foaf:name":[{"@value":"B. McDonald"}],"jpcoar:affiliationName":[{"@value":"John de Laeter Centre, The Institute of Geoscience Research Curtin University  Perth Western Australia Australia"}]},{"@id":"https://cir.nii.ac.jp/crid/1380285708268515843","@type":"Researcher","foaf:name":[{"@value":"N. J. Evans"}],"jpcoar:affiliationName":[{"@value":"Earth Dynamics Research Group, The Institute of Geoscience Research, School of Earth and Planetary Sciences Curtin University  Perth Western Australia Australia"},{"@value":"John de Laeter Centre, The Institute of Geoscience Research Curtin University  Perth Western Australia Australia"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00948276"},{"@type":"EISSN","@value":"19448007"}],"prism:publicationName":[{"@value":"Geophysical Research Letters"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"2019-02-02","prism:volume":"46","prism:number":"3","prism:startingPage":"1259","prism:endingPage":"1267"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2018GL080579"},{"@id":"https://onlinelibrary.wiley.com/doi/pdf/10.1029/2018GL080579"},{"@id":"https://onlinelibrary.wiley.com/doi/full-xml/10.1029/2018GL080579"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/am-pdf/10.1029/2018GL080579"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2018GL080579"}],"createdAt":"2019-01-19","modifiedAt":"2025-05-16","foaf:topic":[{"@id":"https://cir.nii.ac.jp/all?q=550","dc:title":"550"}],"project":[{"@id":"https://cir.nii.ac.jp/crid/1040282256888123520","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"16K05617"},{"@type":"JGN","@value":"JP16K05617"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-16K05617/"}],"notation":[{"@language":"ja","@value":"第四紀花崗岩の生成過程・テクトニクスの解明"},{"@language":"en","@value":"Clarification of magmatic and tectonic evolution of Quaternary granite"}]}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050574036190838272","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Solidification depth and crystallization age of the Shiaidani Granodiorite: constraints to the average denudation rate of the Hida Range, central Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1050845760782107904","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"First report of (U–Th)/He thermochronometric data across Northeast Japan Arc: implications for the long-term inelastic deformation"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011144602731392","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Burial and exhumation of Corsica (France) in the light of fission track 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