{"@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/1363670319173203072.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1016/0009-2541(94)90066-3"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:0009254194900663?httpAccept=text/xml"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:0009254194900663?httpAccept=text/plain"}}],"dc:title":[{"@value":"Characterization of spinel peridotites by olivine-spinel compositional relationships: Review and interpretation"}],"description":[{"notation":[{"@value":"Abstract   A comprehensive review on igneous petrological characteristics of mantle-derived spinel peridotites was made on the basis of their olivine-spinel compositional relationships. The spinel peridotites (harzburgites and lherzolites), of both massif and xenolithic derivations, plot in a narrow band, the olivine-spinel mantle array, in terms of Fo of olivine and C# (   Cr  (Cr+Al)    atomic ratio) of chromian spinel. The Cr# of spinel grows rapidly within the olivine-spinel mantle array with a slight increase of Fo. Their    Cpx  (Opx+Cpx)    volume ratio decreases towards the high-Fo, high-Cr# end; it is 0.1 for Cr#=0.5−0.6. Peridotite suites from each tectonic setting lie in a particular part of the olivine-spinel mantle array.  The olivine-spinel mantle array possibly consists of integrated FoCr# residual trends formed at various conditions ( P  total  and  P  H 2 O ). Cr# of residual spinel coexisting with olivine of a particular Fo increases with a decrease of  P  total  and/or with an increase of  P  H 2 O  on partial melting. Origins of peridotite suites can be constrained to some extent in terms of the FoCr# residual trends, for example, some of the Japan-arc mantle peridotites and fore-arc peridotites are low-pressure and/or hydrous restites, and subcontinental and oceanic hot-spot peridotites are high-pressure and/or anhydrous restites. Fertile alpine-type lherzolites with Cr#≈0.1 are of subcontinental origin. Other alpine lherzolites are most frequently of sub-arc origin, sometimes of sub-ocean floor origin, and rarely of sub-continental origin. Most of the alpine-type harzburgites are of fore-arc origin."}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1383670319173203072","@type":"Researcher","foaf:name":[{"@value":"Shoji Arai"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00092541"},{"@type":"PISSN","@value":"https://id.crossref.org/issn/00092541"}],"prism:publicationName":[{"@value":"Chemical Geology"}],"dc:publisher":[{"@value":"Elsevier BV"}],"prism:publicationDate":"1994-04","prism:volume":"113","prism:number":"3-4","prism:startingPage":"191","prism:endingPage":"204"},"reviewed":"false","dc:rights":["https://www.elsevier.com/tdm/userlicense/1.0/"],"url":[{"@id":"https://api.elsevier.com/content/article/PII:0009254194900663?httpAccept=text/xml"},{"@id":"https://api.elsevier.com/content/article/PII:0009254194900663?httpAccept=text/plain"}],"createdAt":"2003-08-06","modifiedAt":"2019-03-16","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050001338868540416","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Direct evidence for upper mantle structure in the NW Pacific Plate : Microstructural analysis of a petit-spot peridotite xenolith"},{"@value":"Direct evidence for upper mantle structure within the NW Pacific Plate: microstructural analyses of a petit-spot peridotite 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