{"@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/1362262943790770048.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1046/j.1468-8123.2002.00042.x"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1046%2Fj.1468-8123.2002.00042.x"}},{"identifier":{"@type":"URI","@value":"https://onlinelibrary.wiley.com/doi/pdf/10.1046/j.1468-8123.2002.00042.x"}}],"dc:title":[{"@value":"The origins of salinity in metamorphic fluids"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Abstract</jats:title><jats:p>Evaluation of data on formation waters and metamorphic fluids sampled by drilling or preserved in fluid inclusions reveals little correlation between fluid salinity and metamorphic grade, but a strong link to original sedimentary setting. Sediments and metasediments deposited originally in shallow marine environments can contain fluids with a very wide range of salinities, but they are commonly near twice seawater salinity or higher. With increasing metamorphic grade, a very wide range of salinities may develop, with the highest levels tracking halite saturation. Oceanic and accretionary prism sequences yield low‐salinity fluids, close to seawater values, almost irrespective of metamorphic grade until extreme conditions are reached where removal of water may increase fluid salinity. The salinities of metamorphic fluids exert a fundamental control on both fluid phase equilibria and metal‐transporting capability, and appear, to a large degree, to reflect the original presence or absence of highly saline formation waters and/or evaporites in the initial sedimentary sequence.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380004236799393039","@type":"Researcher","foaf:name":[{"@value":"B. W. D. Yardley"}]},{"@id":"https://cir.nii.ac.jp/crid/1382262943790770049","@type":"Researcher","foaf:name":[{"@value":"J. T. Graham"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"14688115"},{"@type":"EISSN","@value":"14688123"}],"prism:publicationName":[{"@value":"Geofluids"}],"dc:publisher":[{"@value":"Wiley"}],"prism:publicationDate":"2002-11","prism:volume":"2","prism:number":"4","prism:startingPage":"249","prism:endingPage":"256"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1046%2Fj.1468-8123.2002.00042.x"},{"@id":"https://onlinelibrary.wiley.com/doi/pdf/10.1046/j.1468-8123.2002.00042.x"}],"createdAt":"2003-03-11","modifiedAt":"2023-10-17","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050564285772252160","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Geochemical features and relative B–Li–Cl compositions of deep-origin fluids trapped in high-pressure metamorphic rocks"}]},{"@id":"https://cir.nii.ac.jp/crid/1050857235853799168","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Megathrust Shear Modulated by Albite Metasomatism in Subduction Mélanges"}]},{"@id":"https://cir.nii.ac.jp/crid/1360025429420974208","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Experimental constraints on serpentinite carbonation in the presence of a H2O–CO2–NaCl fluid"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285704777560576","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Adhesion energy between mica surfaces: Implications for the frictional coefficient under dry and wet conditions"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567181183793920","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Electrical conductivity of NaCl-bearing aqueous fluids to 600 °C and 1 GPa"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567182088817024","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Electrical conductivity of albite–(quartz)–water and albite–water–NaCl systems and its implication to the high conductivity anomalies in the continental crust"}]},{"@id":"https://cir.nii.ac.jp/crid/2051714792046916224","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Electrical conductivity of brine-bearing quartzite at 1 GPa : implications for fluid content and salinity of the crust"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1046/j.1468-8123.2002.00042.x"},{"@type":"CROSSREF","@value":"10.1186/1880-5981-66-2_references_DOI_Becy0mZ1srrWWra7jsSnJVP9vm"},{"@type":"CROSSREF","@value":"10.1016/j.lithos.2015.03.002_references_DOI_Becy0mZ1srrWWra7jsSnJVP9vm"},{"@type":"CROSSREF","@value":"10.1007/s00410-024-02175-4_references_DOI_1rCx018awp2z7Umty7inex2UB74"},{"@type":"CROSSREF","@value":"10.1002/2013jb010550_references_DOI_Becy0mZ1srrWWra7jsSnJVP9vm"},{"@type":"CROSSREF","@value":"10.1029/2022gc010569_references_DOI_Becy0mZ1srrWWra7jsSnJVP9vm"},{"@type":"CROSSREF","@value":"10.1007/s00410-016-1323-z_references_DOI_Becy0mZ1srrWWra7jsSnJVP9vm"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2014.12.021_references_DOI_Becy0mZ1srrWWra7jsSnJVP9vm"}]}