{"@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/1361418520984201600.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1016/0301-9268(95)00066-6"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:0301926895000666?httpAccept=text/xml"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:0301926895000666?httpAccept=text/plain"}}],"dc:title":[{"@value":"The Itsaq Gneiss Complex of southern West Greenland; the world's most extensive record of early crustal evolution (3900-3600 Ma)"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1381418520984201603","@type":"Researcher","foaf:name":[{"@value":"Allen P. Nutman"}]},{"@id":"https://cir.nii.ac.jp/crid/1381418520984201604","@type":"Researcher","foaf:name":[{"@value":"Victor R. McGregor"}]},{"@id":"https://cir.nii.ac.jp/crid/1381418520984201600","@type":"Researcher","foaf:name":[{"@value":"Clark R.L. Friend"}]},{"@id":"https://cir.nii.ac.jp/crid/1381418520984201601","@type":"Researcher","foaf:name":[{"@value":"Victoria C. Bennett"}]},{"@id":"https://cir.nii.ac.jp/crid/1381418520984201602","@type":"Researcher","foaf:name":[{"@value":"Peter D. Kinny"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"03019268"}],"prism:publicationName":[{"@value":"Precambrian Research"}],"dc:publisher":[{"@value":"Elsevier BV"}],"prism:publicationDate":"1996-05","prism:volume":"78","prism:number":"1-3","prism:startingPage":"1","prism:endingPage":"39"},"reviewed":"false","dc:rights":["https://www.elsevier.com/tdm/userlicense/1.0/"],"url":[{"@id":"https://api.elsevier.com/content/article/PII:0301926895000666?httpAccept=text/xml"},{"@id":"https://api.elsevier.com/content/article/PII:0301926895000666?httpAccept=text/plain"}],"createdAt":"2002-07-25","modifiedAt":"2019-04-17","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050845760790441472","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Influence of contamination on banded iron formations in the Isua supracrustal belt, West Greenland: Reevaluation of the Eoarchean seawater compositions"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002215942315520","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The naked planet Earth: Most essential pre-requisite for the origin and evolution of life"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002215942334208","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"A prolonged granitoid formation in Saglek Block, Labrador: Zonal growth and crustal reworking of continental crust in the Eoarchean"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004232523420800","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Geology of the Eoarchean, > 3.95 Ga, Nulliak supracrustal rocks in the Saglek Block, northern Labrador, Canada: The oldest geological evidence for plate tectonics"}]},{"@id":"https://cir.nii.ac.jp/crid/1360009142703973248","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Occurrence and chemical composition of the Eoarchean carbonate rocks of the Nulliak supracrustal rocks in the Saglek Block of northeastern Labrador, Canada"}]},{"@id":"https://cir.nii.ac.jp/crid/1360013168823838336","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Deserpentinization and high-pressure (eclogite-facies) metamorphic features in the Eoarchean ultramafic body from Isua, Greenland"}]},{"@id":"https://cir.nii.ac.jp/crid/1360283690913992320","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Rhenium-osmium isotopes and highly siderophile elements in ultramafic rocks from the Eoarchean Saglek Block, northern Labrador, Canada: implications for Archean mantle evolution"}]},{"@id":"https://cir.nii.ac.jp/crid/1360286993335901568","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Ruthenium isotope vestige of Earth’s pre-late-veneer mantle preserved in Archaean rocks"}]},{"@id":"https://cir.nii.ac.jp/crid/1360306905631116160","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Komatiitic parental magmas of the Archean Ujaragssuit Nunât ultramafic body, SW Greenland, identified from spinel chemistry"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567182004463232","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"In-situ iron isotope analysis of pyrites in ~ 3.7 Ga sedimentary protoliths from the Isua supracrustal belt, southern West Greenland"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567182409712896","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Occurrence and geochronology of the Eoarchean, ∼3.9 Ga, Iqaluk Gneiss in the Saglek Block, northern Labrador, Canada: Evidence for the oldest supracrustal rocks in the world"}]},{"@id":"https://cir.nii.ac.jp/crid/1360580232181747968","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Evolution of the Archean felsic crust of Singhbhum Craton, India: A reassessment"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848657236224256","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The Archean Victoria Fjord terrane of northernmost Greenland and geodynamic interpretation of Precambrian crust in and surrounding the Arctic Ocean"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848657386429824","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Petrology and geochemistry of mafic rocks in the Acasta Gneiss Complex: Implications for the oldest mafic rocks and their origin"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848657453555328","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Intermediate P/T-type regional metamorphism of the Isua Supracrustal Belt, southern west Greenland: The oldest Pacific-type orogenic belt?"}]},{"@id":"https://cir.nii.ac.jp/crid/1360865815671514624","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Zircon within chromitite requires revision of the tectonic history of the Eoarchean Itsaq Gneiss complex, Greenland"}]},{"@id":"https://cir.nii.ac.jp/crid/1361975840682877696","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Implications for the origins of Eoarchean ultramafic rocks of the North Atlantic Craton: a study of the Tussaap Ultramafic complex, Itsaq Gneiss complex, southern West Greenland"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282763068365696","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"カナダ，ラブラドル・ヌリアック表成岩類の地質と年代"},{"@language":"en","@value":"Geology and Geochronology of Nulliak Supracrustal Rocks in Labrador, Canada: The Oldest Supracrustal Rocks and Evidence for the Operation of Plate Tectonics"},{"@value":"カナダ,ラブラドル・ヌリアック表成岩類の地質と年代 : 地球最古の表成岩とプレートテクトニクスの証拠"},{"@language":"ja-Kana","@value":"カナダ,ラブラドル ・ ヌリアックヒョウセイガンルイ ノ チシツ ト ネンダイ : チキュウ サイコ ノ ヒョウセイガン ト プレートテクトニクス ノ ショウコ"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1016/0301-9268(95)00066-6"},{"@type":"CROSSREF","@value":"10.1111/iar.12381_references_DOI_LQGSNvTFhabpafFEBfzUNkzYbPe"},{"@type":"CROSSREF","@value":"10.5026/jgeography.127.683_references_DOI_LQGSNvTFhabpafFEBfzUNkzYbPe"},{"@type":"CROSSREF","@value":"10.1016/j.gsf.2021.101298_references_DOI_LQGSNvTFhabpafFEBfzUNkzYbPe"},{"@type":"CROSSREF","@value":"10.1038/s41586-020-2069-3_references_DOI_LQGSNvTFhabpafFEBfzUNkzYbPe"},{"@type":"CROSSREF","@value":"10.1016/j.gca.2017.07.023_references_DOI_LQGSNvTFhabpafFEBfzUNkzYbPe"},{"@type":"CROSSREF","@value":"10.1007/s00410-025-02208-6_references_DOI_LQGSNvTFhabpafFEBfzUNkzYbPe"},{"@type":"CROSSREF","@value":"10.1016/j.tecto.2015.05.003_references_DOI_LQGSNvTFhabpafFEBfzUNkzYbPe"},{"@type":"CROSSREF","@value":"10.1016/j.chemgeo.2015.02.022_references_DOI_LQGSNvTFhabpafFEBfzUNkzYbPe"},{"@type":"CROSSREF","@value":"10.1016/j.precamres.2016.03.018_references_DOI_LQGSNvTFhabpafFEBfzUNkzYbPe"},{"@type":"CROSSREF","@value":"10.1016/j.precamres.2016.07.004_references_DOI_LQGSNvTFhabpafFEBfzUNkzYbPe"},{"@type":"CROSSREF","@value":"10.1016/j.earscirev.2022.104067_references_DOI_LQGSNvTFhabpafFEBfzUNkzYbPe"},{"@type":"CROSSREF","@value":"10.1016/j.gsf.2016.06.013_references_DOI_LQGSNvTFhabpafFEBfzUNkzYbPe"},{"@type":"CROSSREF","@value":"10.1016/j.gsf.2023.101648_references_DOI_LQGSNvTFhabpafFEBfzUNkzYbPe"},{"@type":"CROSSREF","@value":"10.1016/j.jog.2019.03.006_references_DOI_LQGSNvTFhabpafFEBfzUNkzYbPe"},{"@type":"CROSSREF","@value":"10.1016/j.gsf.2012.11.001_references_DOI_LQGSNvTFhabpafFEBfzUNkzYbPe"},{"@type":"CROSSREF","@value":"10.1007/s00410-019-1628-9_references_DOI_LQGSNvTFhabpafFEBfzUNkzYbPe"},{"@type":"CROSSREF","@value":"10.1016/j.tecto.2015.05.020_references_DOI_LQGSNvTFhabpafFEBfzUNkzYbPe"},{"@type":"CROSSREF","@value":"10.1016/j.gsf.2016.11.016_references_DOI_LQGSNvTFhabpafFEBfzUNkzYbPe"}]}