{"@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/1360004232174023936.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1016/j.gsf.2013.04.003"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S167498711300056X?httpAccept=text/xml"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S167498711300056X?httpAccept=text/plain"}},{"identifier":{"@type":"HANDLE","@value":"20.500.11937/2863"}}],"resourceType":"学術雑誌論文(journal article)","dc:title":[{"@value":"Petrology and SHRIMP zircon geochronology of granulites from Vesleknausen, Lützow-Holm Complex, East Antarctica: Neoarchean magmatism and Neoproterozoic high-grade metamorphism"}],"description":[{"notation":[{"@value":"AbstractWe report new petrological data and geochronological measurements of granulites from Vesleknausen in the highest-grade section of the Lützow-Holm Complex, part of the Gondwana-assembling collisional orogen in East Antarctica. The locality is dominated by felsic to intermediate orthogneiss (charnockite and minor biotite gneiss), mafic orthogneiss, and hornblende-pyroxene granulite, with deformed and undeformed dykes of metagranite and felsic pegmatite. Pseudosection analysis of charnockite in the system NCKFMASHTO, supported by geothermometry of mafic orthogneiss, was used to infer peak metamorphic temperatures of 750–850 °C, approximately 150 °C lower than those estimated for metasedimentary gneisses from Rundvågshetta, 6 km to the northeast. SHRIMP U-Pb analysis of zircons from feldspar-pyroxene gneiss, which corresponds to a partially molten patch around mafic orthogneiss, yielded a Concordia upper intercept ages of 2507.9 ± 7.4 Ma, corresponding to the time of formation of the magmatic protolith to the orthogneiss. Partial melting during peak metamorphism probably took place between 591 and 548 Ma, as recorded in rims overgrew around magmatic zircon. Our results suggest that Rundvågshetta-Vesleknausen-Strandnibba region in southwestern Lützow-Holm Bay, where orthogneisses are dominant, consists of a single crustal block, possibly formed by ca. 2.5 Ga arc magmatism. The Neoarchean magmatic terrane was tectonically mingled with other fragments (such as metasedimentary units in northern Lützow-Holm Bay) by subduction/collision events during the assembly of Gondwana supercontinent, and subsequently underwent ∼850 °C granulite-facies metamorphosed during Neoproterozoic to Cambrian final collisional event."}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380004232174023938","@type":"Researcher","foaf:name":[{"@value":"Daniel J. Dunkley"}]},{"@id":"https://cir.nii.ac.jp/crid/1420845751162614272","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"50252888"},{"@type":"NRID","@value":"1000050252888"},{"@type":"ORCID","@value":"0000-0003-1606-5717"},{"@type":"NRID","@value":"9000021297345"},{"@type":"NRID","@value":"9000001319463"},{"@type":"NRID","@value":"9000282394775"},{"@type":"NRID","@value":"9000002218701"},{"@type":"NRID","@value":"9000283728402"},{"@type":"NRID","@value":"9000242078420"},{"@type":"NRID","@value":"9000403551578"},{"@type":"NRID","@value":"9000002018222"},{"@type":"NRID","@value":"9000391814767"},{"@type":"NRID","@value":"9000409995873"},{"@type":"NRID","@value":"9000392820574"},{"@type":"NRID","@value":"9000322669146"},{"@type":"NRID","@value":"9000015504943"},{"@type":"NRID","@value":"9000406039758"},{"@type":"NRID","@value":"9000000786567"},{"@type":"NRID","@value":"9000001848199"},{"@type":"NRID","@value":"9000406039933"},{"@type":"NRID","@value":"9000002142751"},{"@type":"NRID","@value":"9000022836725"},{"@type":"NRID","@value":"9000335196235"},{"@type":"NRID","@value":"9000386338286"},{"@type":"NRID","@value":"9000022838687"},{"@type":"NRID","@value":"9000022838554"},{"@type":"NRID","@value":"9000254146502"},{"@type":"NRID","@value":"9000002103230"},{"@type":"NRID","@value":"9000002142748"},{"@type":"NRID","@value":"9000406038241"},{"@type":"NRID","@value":"9000401434288"},{"@type":"NRID","@value":"9000002218443"},{"@type":"NRID","@value":"9000002017784"},{"@type":"NRID","@value":"9000386337899"},{"@type":"NRID","@value":"9000347137209"},{"@type":"NRID","@value":"9000347083360"},{"@type":"NRID","@value":"9000413505011"},{"@type":"NRID","@value":"9000347167058"},{"@type":"NRID","@value":"9000347668577"},{"@type":"NRID","@value":"9000386338098"},{"@type":"NRID","@value":"9000347083128"},{"@type":"NRID","@value":"9000001319502"},{"@type":"NRID","@value":"9000016434222"},{"@type":"NRID","@value":"9000386337785"},{"@type":"NRID","@value":"9000347167186"},{"@type":"NRID","@value":"9000258432765"},{"@type":"NRID","@value":"9000396138753"},{"@type":"NRID","@value":"9000406038213"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/tsunogae"}],"foaf:name":[{"@value":"Toshiaki Tsunogae"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004232174023939","@type":"Researcher","foaf:name":[{"@value":"Takahiro Endo"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004232174023936","@type":"Researcher","foaf:name":[{"@value":"Kenji Horie"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004232174023940","@type":"Researcher","foaf:name":[{"@value":"Tomoharu Miyamoto"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004232174023808","@type":"Researcher","foaf:name":[{"@value":"Mutsumi Kato"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"16749871"},{"@type":"PISSN","@value":"https://id.crossref.org/issn/16749871"},{"@type":"PISSN","@value":"http://id.crossref.org/issn/16749871"}],"prism:publicationName":[{"@value":"Geoscience Frontiers"}],"dc:publisher":[{"@value":"Elsevier BV"}],"prism:publicationDate":"2014-03","prism:volume":"5","prism:number":"2","prism:startingPage":"167","prism:endingPage":"182"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","dc:rights":["https://www.elsevier.com/tdm/userlicense/1.0/","http://creativecommons.org/licenses/by-nc-nd/3.0/"],"url":[{"@id":"https://api.elsevier.com/content/article/PII:S167498711300056X?httpAccept=text/xml"},{"@id":"https://api.elsevier.com/content/article/PII:S167498711300056X?httpAccept=text/plain"}],"createdAt":"2013-04-28","modifiedAt":"2018-10-16","foaf:topic":[{"@id":"https://cir.nii.ac.jp/all?q=550","dc:title":"550"},{"@id":"https://cir.nii.ac.jp/all?q=Charnockite","dc:title":"Charnockite"},{"@id":"https://cir.nii.ac.jp/all?q=Pseudosection","dc:title":"Pseudosection"},{"@id":"https://cir.nii.ac.jp/all?q=Earth%20and%20Planetary%20Sciences(all)","dc:title":"Earth and Planetary Sciences(all)"},{"@id":"https://cir.nii.ac.jp/all?q=SHRIMP%20zircon%20geochronology","dc:title":"SHRIMP zircon geochronology"},{"@id":"https://cir.nii.ac.jp/all?q=Gondwana%20supercontinent","dc:title":"Gondwana supercontinent"},{"@id":"https://cir.nii.ac.jp/all?q=Granulite","dc:title":"Granulite"},{"@id":"https://cir.nii.ac.jp/all?q=Rundv%C3%A5gshetta%20-%20Gondwana%20supercontinent","dc:title":"Rundvågshetta - Gondwana supercontinent"},{"@id":"https://cir.nii.ac.jp/all?q=Rundv%C3%A5gshetta","dc:title":"Rundvågshetta"}],"project":[{"@id":"https://cir.nii.ac.jp/crid/1040000782113742208","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"22403017"},{"@type":"JGN","@value":"JP22403017"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-22403017/"}],"notation":[{"@language":"ja","@value":"南極―インド―マダガスカル地域の岩石学的精密解析とゴンドワナ超大陸の形成"},{"@language":"en","@value":"Petrological study of granulites from Antarctica-India-Madagascar region and the formation of the Gondwana Supercontinent"}]},{"@id":"https://cir.nii.ac.jp/crid/1040000782425754752","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"12J04821"},{"@type":"JGN","@value":"JP12J04821"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-12J04821/"}],"notation":[{"@language":"ja","@value":"地殻深部の異種岩石間の相互作用の研究 : 岩石の部分融解とその役割の解明"}]},{"@id":"https://cir.nii.ac.jp/crid/1040282257219898240","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"25287132"},{"@type":"JGN","@value":"JP25287132"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-25287132/"}],"notation":[{"@language":"ja","@value":"地殻形成素過程解明に向けた微小領域高精度ジルコン年代測定の実証研究"},{"@language":"en","@value":"Geochronological study of high precision zircon microanalysis for crustal evolution"}]}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050007857358719488","@type":"Article","resourceType":"学術雑誌論文(journal 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ultrahigh-temperature metamorphism at Rundvågshetta, Lützow-Holm Complex, East Antarctica"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855570736235520","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Cambrian Orogenic Belt in East Antarctica and Sri Lanka: Implications for Gondwana Assembly"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855571132402048","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Magmatic evolution and tectonic setting of metabasites from Lützow-Holm Complex, East Antarctica"}]},{"@id":"https://cir.nii.ac.jp/crid/1360865814725668096","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Petrology and geochronology of sapphirine‐bearing granulites from the Limpopo Complex in eastern Botswana: Implications for Palaeoproterozoic long‐lived high‐pressure/ultrahigh‐temperature metamorphism and rapid exhumation"}]},{"@id":"https://cir.nii.ac.jp/crid/1360865814728687360","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Reply to ‘Comment on “Neoarchean arc magmatism and Paleoproterozoic high-pressure granulite-facies metamorphism in the southern Motloutse Complex, eastern Botswana: Implication for the western extension of the Limpopo Complex”’ by Mfa et al."}]},{"@id":"https://cir.nii.ac.jp/crid/1360865815484801280","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Charnockites: Petrologic and phase equilibria characterization of some global examples"}]},{"@id":"https://cir.nii.ac.jp/crid/1361137043618358400","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"U‐Pb geochronology of zircons from lunar breccia 73217 using a sensitive high mass‐resolution ion 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