{"@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/1362262943337915264.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1016/s0012-821x(00)00038-8"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0012821X00000388?httpAccept=text/xml"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0012821X00000388?httpAccept=text/plain"}}],"dc:title":[{"@value":"Garnet fractionation in a hydrous magma ocean and the origin of Al-depleted komatiites: melting experiments of hydrous pyrolite with REEs at high pressure"}],"description":[{"notation":[{"@value":"Abstract   Melting experiments of a representative mantle composition doped with some key trace elements were conducted under hydrous conditions at pressures to 20 GPa. The results demonstrate that only ∼5–25% of garnet fractionation and relatively low pressures ( 3.5 Ga) in the solidifying hydrous magma ocean. This suggests that the Archean mantle was much cooler than so far believed from the origin of the komatiites based on anhydrous experiments."}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1420845751157161984","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"00291500"},{"@type":"NRID","@value":"1000000291500"},{"@type":"NRID","@value":"9000283727937"},{"@type":"NRID","@value":"9000410511413"},{"@type":"NRID","@value":"9000401431373"},{"@type":"NRID","@value":"9000008731900"},{"@type":"NRID","@value":"9000262360223"},{"@type":"NRID","@value":"9000370282002"},{"@type":"NRID","@value":"9000303159614"},{"@type":"NRID","@value":"9000286626669"},{"@type":"NRID","@value":"9000014613724"},{"@type":"NRID","@value":"9000392598264"},{"@type":"NRID","@value":"9000003589615"},{"@type":"NRID","@value":"9000411371718"},{"@type":"NRID","@value":"9000008234809"},{"@type":"NRID","@value":"9000054225459"},{"@type":"NRID","@value":"9000408904798"},{"@type":"NRID","@value":"9000019059246"},{"@type":"NRID","@value":"9000408918920"},{"@type":"NRID","@value":"9000258403332"},{"@type":"NRID","@value":"9000256598476"},{"@type":"NRID","@value":"9000001806975"},{"@type":"NRID","@value":"9000406039400"},{"@type":"NRID","@value":"9000004971410"},{"@type":"NRID","@value":"9000014283690"},{"@type":"NRID","@value":"9000267786314"},{"@type":"NRID","@value":"9000254201214"},{"@type":"NRID","@value":"9000312255237"},{"@type":"NRID","@value":"9000310331227"},{"@type":"NRID","@value":"9000345400743"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/Toru_Inoue"}],"foaf:name":[{"@value":"Toru Inoue"}]},{"@id":"https://cir.nii.ac.jp/crid/1382262943337915266","@type":"Researcher","foaf:name":[{"@value":"Robert P Rapp"}]},{"@id":"https://cir.nii.ac.jp/crid/1382262943337915267","@type":"Researcher","foaf:name":[{"@value":"Jianzhong Zhang"}]},{"@id":"https://cir.nii.ac.jp/crid/1382262943337915268","@type":"Researcher","foaf:name":[{"@value":"Tibor Gasparik"}]},{"@id":"https://cir.nii.ac.jp/crid/1382262943337915264","@type":"Researcher","foaf:name":[{"@value":"Donald J Weidner"}]},{"@id":"https://cir.nii.ac.jp/crid/1382262943337915269","@type":"Researcher","foaf:name":[{"@value":"Tetsuo Irifune"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"0012821X"}],"prism:publicationName":[{"@value":"Earth and Planetary Science Letters"}],"dc:publisher":[{"@value":"Elsevier BV"}],"prism:publicationDate":"2000-04-15","prism:volume":"177","prism:number":"1-2","prism:startingPage":"81","prism:endingPage":"87"},"reviewed":"false","dc:rights":["https://www.elsevier.com/tdm/userlicense/1.0/"],"url":[{"@id":"https://api.elsevier.com/content/article/PII:S0012821X00000388?httpAccept=text/xml"},{"@id":"https://api.elsevier.com/content/article/PII:S0012821X00000388?httpAccept=text/plain"}],"createdAt":"2002-07-25","modifiedAt":"2019-04-14","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1390001206524731264","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"High pressure and high temperature experimental studies for the effect of water on the Earth's mantle minerals"},{"@language":"ja","@value":"高温高圧実験によるマントル鉱物における水の影響に関する研究"},{"@value":"日本鉱物科学会賞第5回受賞者 受賞記念研究紹介 高温高圧実験によるマントル鉱物における水の影響に関する研究"},{"@language":"ja-Kana","@value":"ニホン コウブツ カガクカイショウ ダイ5カイ ジュショウシャ ジュショウ キネン ケンキュウ ショウカイ コウオン コウアツ ジッケン ニ ヨル マントル コウブツ ニ オケル ミズ ノ エイキョウ ニ カンスル ケンキュウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679358493312","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Hydrogenation of FeSi and FeS Alloys at High Pressure and High Temperature"},{"@language":"ja","@value":"高温高圧下におけるＦｅＳｉおよびＦｅＳ合金の水素化"},{"@language":"ja-Kana","@value":"コウオン コウアツカ ニ オケル FeSi オヨビ FeS ゴウキン ノ スイソカ"}]},{"@id":"https://cir.nii.ac.jp/crid/2051714791861480448","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Hydrogen-rich hydrothermal environments in the Hadean ocean inferred from serpentinization of komatiites at 300 ℃ and 500 bar"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1016/s0012-821x(00)00038-8"},{"@type":"OPENAIRE","@value":"doi_dedup___::d595398c0f19df96cffa2dfa3cf60073"},{"@type":"CROSSREF","@value":"10.1186/s40645-015-0076-z_references_DOI_J6GaLu95pwwbM6q68RzJ0kJ85KD"},{"@type":"CROSSREF","@value":"10.2465/gkk.110111_references_DOI_J6GaLu95pwwbM6q68RzJ0kJ85KD"},{"@type":"CROSSREF","@value":"10.4131/jshpreview.21.197_references_DOI_J6GaLu95pwwbM6q68RzJ0kJ85KD"}]}