{"@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/1362262944807101440.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1016/0016-7037(95)00215-l"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:001670379500215L?httpAccept=text/xml"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:001670379500215L?httpAccept=text/plain"}}],"dc:title":[{"@value":"Mineral-aqueous fluid partitioning of trace elements at 900°C and 2.0 GPa: Constraints on the trace element chemistry of mantle and deep crustal fluids"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380004236799454480","@type":"Researcher","foaf:name":[{"@value":"J.M. Brenan"}]},{"@id":"https://cir.nii.ac.jp/crid/1382262944807101443","@type":"Researcher","foaf:name":[{"@value":"H.F. Shaw"}]},{"@id":"https://cir.nii.ac.jp/crid/1382262944807101441","@type":"Researcher","foaf:name":[{"@value":"F.J. Ryerson"}]},{"@id":"https://cir.nii.ac.jp/crid/1382262944807101440","@type":"Researcher","foaf:name":[{"@value":"D.L. Phinney"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00167037"}],"prism:publicationName":[{"@value":"Geochimica et Cosmochimica Acta"}],"dc:publisher":[{"@value":"Elsevier BV"}],"prism:publicationDate":"1995-08","prism:volume":"59","prism:number":"16","prism:startingPage":"3331","prism:endingPage":"3350"},"reviewed":"false","dc:rights":["https://www.elsevier.com/tdm/userlicense/1.0/"],"url":[{"@id":"https://api.elsevier.com/content/article/PII:001670379500215L?httpAccept=text/xml"},{"@id":"https://api.elsevier.com/content/article/PII:001670379500215L?httpAccept=text/plain"}],"createdAt":"2002-07-26","modifiedAt":"2019-04-15","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360002215942218752","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Isotopic heterogeneity of oceanic, arc and continental basalts and its implications for mantle dynamics"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285707282785408","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Miocene-Pliocene mantle depletion event in the northern Fossa Magna, western NE Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285707326375296","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Aqueous fluids and sedimentary melts as agents for mantle wedge metasomatism, as inferred from peridotite xenoliths at Pinatubo and Iraya volcanoes, Luzon arc, Philippines"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285707326408960","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Petrogenesis of an Early Cretaceous lamprophyre dike from Kyoto Prefecture, Japan: Implications for the generation of high-Nb basalt magmas in subduction zones"}]},{"@id":"https://cir.nii.ac.jp/crid/1360584341819498624","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Compositional evolution of slab-derived fluids during ascent: implications from trace-element partition between hydrous melts and Cl-free or Cl-rich aqueous fluids"}]},{"@id":"https://cir.nii.ac.jp/crid/1360588379392413568","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"A HIMU-like component in Mariana Convergent Margin magma sources during initial arc rifting revealed by melt inclusions"}]},{"@id":"https://cir.nii.ac.jp/crid/1360846640846286720","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The effect of sediment recycling in subduction zones on the Hf isotope character of new arc crust, Banda arc, Indonesia"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848657279702400","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Mineral chemistry of the Neoproterozoic Alaskan-type Akarem Intrusion with special emphasis on amphibole: Implications for the pluton origin and evolution of subduction-related magma"}]},{"@id":"https://cir.nii.ac.jp/crid/1360853567603544960","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Petrogenetic constraints on magma fertility in the Baguio Mineral District, Philippines: Probing the mineralization potential of the igneous host rocks in the Sangilo epithermal deposit"}]},{"@id":"https://cir.nii.ac.jp/crid/1360857593727300736","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Simultaneous Analysis of Seismic Velocity and Electrical Conductivity in the Crust and the Uppermost Mantle: A Forward Model and Inversion Test Based on Grid Search"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204155424512","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"230Th/238U and 226Ra/230Th Activity Ratios in Rhyolite from Izu Arc Volcanoes"},{"@language":"ja","@value":"伊豆弧の火山から噴出した流紋岩中の<SUP>230</SUP>Th/<SUP>238</SUP>Uと<SUP>226</SUP>Ra/<SUP>230</SUP>Thの放射能強度比"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204155736576","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"238U-230Th-226Ra Radioactive Disequilibria in the Lava Flows of the 1986 Eruption from Izu-Oshima Volcano, Japan"},{"@language":"ja","@value":"伊豆大島火山1986年溶岩流の <SUP>238</SUP>U-<SUP>230</SUP>Th-<SUP>226</SUP>Ra放射非平衡"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204554178432","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"East-west mantle geochemical hemispheres constrained from Independent Component Analysis of basalt isotopic compositions"},{"@value":"East–west geochemical hemispheres anchored to asthenosphere in the Earth's mantle"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204554620928","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Boron systematics of Hisatsu and Kirishima basaltic rocks from southern Kyushu, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206546546688","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Effect of subduction components on production of basalts from Tateshina volcano, central Japan: geochemical calculation of dehydration of subducting oceanic crust and partial melting of overlying sediments, and subsequent fluid-mantle interaction"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679133042944","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"伊豆弧の火山から噴出するマグマ中のウラン系列核種間の放射平衡・非平衡"},{"@language":"en","@value":"Radioactive Equilibria and Disequilibria of U-Series Nuclides in Erupting Magmas from Izu Arc Volcanoes"},{"@language":"ja-Kana","@value":"イズ コ ノ カザン カラ フキダスル マグマ チュウ ノ ウラン ケイレツカクシュ カン ノ ホウシャ ヘイコウ ヒヘイコウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679133085184","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"238U-230Th-226Ra Radioactive Disequilibria in the Products from 1707 Eruption of Fuji Volcano, Japan"},{"@language":"ja","@value":"富士火山1707年噴出物中の<SUP>238</SUP>U-<SUP>230</SUP>Th-<SUP>226</SUP>Ra放射非平衡"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679133866112","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"230Th/238U Activity Ratios in Rhyolite from Izu Arc Volcanoes"},{"@language":"ja","@value":"伊豆弧の火山から噴出した流紋岩中の<sup>230</sup>Th/<sup>238</sup>U放射能強度比"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679526629248","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"238U-230Th radioactive disequilibrium in the northern Izu arc: (230Th/232Th) in the sub-arc mantle"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679526647552","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Trace element and isotopic evidence for temporal changes of the mantle sources in the South Shetland Islands, Antarctica"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681522798976","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Operation of subduction factory and production of andesite"}]},{"@id":"https://cir.nii.ac.jp/crid/1390299915004519040","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Molybdenum isotopic compositions in volcanic rocks from Northern Izu arc (Izu-Oshima, Niijima, and Kozushima)"}]},{"@id":"https://cir.nii.ac.jp/crid/1390573242692873984","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Geochronology and geochemistry of granitoids from the Mongolian Altai"}]},{"@id":"https://cir.nii.ac.jp/crid/2051433317070229760","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Arima hot spring waters as a deep-seated brine from subducting slab"}]},{"@id":"https://cir.nii.ac.jp/crid/2051714792046927360","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Large-ion lithophile elements delivered by saline fluids to the sub-arc mantle"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1016/0016-7037(95)00215-l"},{"@type":"CROSSREF","@value":"10.1186/1880-5981-66-61_references_DOI_aFjDMtquciXC4AUbnpeK9TmiIu6"},{"@type":"CROSSREF","@value":"10.2343/geochemj.2.0224_references_DOI_aFjDMtquciXC4AUbnpeK9TmiIu6"},{"@type":"CROSSREF","@value":"10.1016/j.gr.2014.09.003_references_DOI_aFjDMtquciXC4AUbnpeK9TmiIu6"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2010.12.053_references_DOI_aFjDMtquciXC4AUbnpeK9TmiIu6"},{"@type":"CROSSREF","@value":"10.3769/radioisotopes.58.599_references_DOI_aFjDMtquciXC4AUbnpeK9TmiIu6"},{"@type":"CROSSREF","@value":"10.1016/j.jog.2016.03.007_references_DOI_aFjDMtquciXC4AUbnpeK9TmiIu6"},{"@type":"CROSSREF","@value":"10.3769/radioisotopes.58.93_references_DOI_aFjDMtquciXC4AUbnpeK9TmiIu6"},{"@type":"CROSSREF","@value":"10.1029/2021jb022307_references_DOI_Umk3bTNxatXNydZVPF3YrVilt63"},{"@type":"CROSSREF","@value":"10.2465/jmps.101.145_references_DOI_aFjDMtquciXC4AUbnpeK9TmiIu6"},{"@type":"CROSSREF","@value":"10.1016/j.lithos.2012.09.015_references_DOI_aFjDMtquciXC4AUbnpeK9TmiIu6"},{"@type":"CROSSREF","@value":"10.2343/geochemj.1.0076_references_DOI_aFjDMtquciXC4AUbnpeK9TmiIu6"},{"@type":"CROSSREF","@value":"10.1016/j.lithos.2016.07.008_references_DOI_aFjDMtquciXC4AUbnpeK9TmiIu6"},{"@type":"CROSSREF","@value":"10.2465/jmps.210830_references_DOI_aFjDMtquciXC4AUbnpeK9TmiIu6"},{"@type":"CROSSREF","@value":"10.1007/s00410-024-02122-3_references_DOI_aFjDMtquciXC4AUbnpeK9TmiIu6"},{"@type":"CROSSREF","@value":"10.1038/s41467-024-48308-y_references_DOI_aFjDMtquciXC4AUbnpeK9TmiIu6"},{"@type":"CROSSREF","@value":"10.2343/geochemj.42.461_references_DOI_aFjDMtquciXC4AUbnpeK9TmiIu6"},{"@type":"CROSSREF","@value":"10.2343/geochemj.42.207_references_DOI_aFjDMtquciXC4AUbnpeK9TmiIu6"},{"@type":"CROSSREF","@value":"10.3769/radioisotopes.57.471_references_DOI_aFjDMtquciXC4AUbnpeK9TmiIu6"},{"@type":"CROSSREF","@value":"10.3769/radioisotopes.58.13_references_DOI_aFjDMtquciXC4AUbnpeK9TmiIu6"},{"@type":"CROSSREF","@value":"10.1186/1880-5981-66-119_references_DOI_aFjDMtquciXC4AUbnpeK9TmiIu6"},{"@type":"CROSSREF","@value":"10.1016/j.oregeorev.2020.103703_references_DOI_aFjDMtquciXC4AUbnpeK9TmiIu6"},{"@type":"CROSSREF","@value":"10.2343/geochemj.gj24005_references_DOI_aFjDMtquciXC4AUbnpeK9TmiIu6"},{"@type":"CROSSREF","@value":"10.2465/jmps.071214_references_DOI_aFjDMtquciXC4AUbnpeK9TmiIu6"},{"@type":"CROSSREF","@value":"10.3769/radioisotopes.58.129_references_DOI_aFjDMtquciXC4AUbnpeK9TmiIu6"},{"@type":"CROSSREF","@value":"10.1016/j.lithos.2017.07.023_references_DOI_aFjDMtquciXC4AUbnpeK9TmiIu6"}]}