{"@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/1363670320499010176.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1016/0016-7037(95)00405-x"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:001670379500405X?httpAccept=text/xml"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:001670379500405X?httpAccept=text/plain"}}],"dc:title":[{"@value":"The role of hydrothermal fluids in the production of subduction zone magmas: Evidence from siderophile and chalcophile trace elements and boron"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1383670320499010179","@type":"Researcher","foaf:name":[{"@value":"P.D. Noll"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670320499010177","@type":"Researcher","foaf:name":[{"@value":"H.E. Newsom"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670320499010176","@type":"Researcher","foaf:name":[{"@value":"W.P. Leeman"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670320499010178","@type":"Researcher","foaf:name":[{"@value":"J.G. Ryan"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00167037"}],"prism:publicationName":[{"@value":"Geochimica et Cosmochimica Acta"}],"dc:publisher":[{"@value":"Elsevier BV"}],"prism:publicationDate":"1996-02","prism:volume":"60","prism:number":"4","prism:startingPage":"587","prism:endingPage":"611"},"reviewed":"false","dc:rights":["https://www.elsevier.com/tdm/userlicense/1.0/"],"url":[{"@id":"https://api.elsevier.com/content/article/PII:001670379500405X?httpAccept=text/xml"},{"@id":"https://api.elsevier.com/content/article/PII:001670379500405X?httpAccept=text/plain"}],"createdAt":"2002-07-25","modifiedAt":"2019-04-22","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360846640787854464","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Thallium isotope systematics in volcanic rocks from St. Helena – Constraints on the origin of the HIMU reservoir"}]},{"@id":"https://cir.nii.ac.jp/crid/1361131416786195840","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The composition of Mars"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204230144000","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Trans-crustal Advections and In-situ Biogeochemical Processes of Global Sub-seafloor Aquifer: The Sub-seafloor “TAIGA”"},{"@value":"海底下の大河"},{"@language":"ja-Kana","@value":"カイテイ カ ノ タイガ カイヨウ チカク ナイ ネッスイ ジュンカン ノ タヨウセイ ト セイブツ チキュウ カガク プロセス"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206525838080","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Crystal chemical behavior of Tl 6s2 lone electron pairs: Inert pair effect imposing constraints on the mineral species."},{"@language":"ja","@value":"Ｔｌ　６ｓ｀２´孤立電子対の結晶化学的挙動　　鉱物種を限定する不活性電子対効果"},{"@value":"Tl6s2孤立電子対の結晶化学的挙動--鉱物種を限定する不活性電子対効果"},{"@language":"ja-Kana","@value":"Tl6s2 コリツ デンシツイ ノ ケッショウ カガクテキ キョドウ コウブツシュ オ ゲンテイ スル フカッセイ デンシツイ コウカ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679530311040","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Boron and other trace element constraints on the slab-derived component in Quaternary volcanic rocks from the Southern Volcanic Zone of the Andes"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681501240960","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Recent developments in crystal chemistry and geochemistry of allanite: Embryo of island arc mineralogy"},{"@language":"ja","@value":"褐簾石の結晶化学と地球化学の最近の動向：島弧鉱物学の萌芽"},{"@value":"岩石鉱物各論 褐簾石の結晶化学と地球化学の最近の動向--島弧鉱物学の萌芽"},{"@language":"ja-Kana","@value":"ガンセキ コウブツ カクロン カツレンセキ ノ ケッショウ カガク ト チキュウ カガク ノ サイキン ノ ドウコウ トウコ コウブツガク ノ ホウガ"}]},{"@id":"https://cir.nii.ac.jp/crid/2050025942135632896","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Arsenic cycling in the Earth’s crust and hydrosphere : interaction between naturally occurring arsenic and human activities"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1016/0016-7037(95)00405-x"},{"@type":"CROSSREF","@value":"10.1016/j.chemgeo.2017.11.025_references_DOI_8eA2dGdDvIT4AD7HA7scPQet4gV"},{"@type":"CROSSREF","@value":"10.5026/jgeography.118.1027_references_DOI_8eA2dGdDvIT4AD7HA7scPQet4gV"},{"@type":"CROSSREF","@value":"10.2465/gkk.30.180_references_DOI_8eA2dGdDvIT4AD7HA7scPQet4gV"},{"@type":"CROSSREF","@value":"10.2465/gkk.37.153_references_DOI_8eA2dGdDvIT4AD7HA7scPQet4gV"},{"@type":"CROSSREF","@value":"10.2343/geochemj.2.0241_references_DOI_8eA2dGdDvIT4AD7HA7scPQet4gV"},{"@type":"CROSSREF","@value":"10.1186/s40645-018-0224-3_references_DOI_8eA2dGdDvIT4AD7HA7scPQet4gV"},{"@type":"CROSSREF","@value":"10.1016/j.gca.2020.01.011_references_DOI_8eA2dGdDvIT4AD7HA7scPQet4gV"}]}