{"@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/1361137045826553344.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1016/s0012-821x(98)00080-6"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0012821X98000806?httpAccept=text/xml"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0012821X98000806?httpAccept=text/plain"}},{"identifier":{"@type":"NAID","@value":"30007236173"}}],"dc:title":[{"@value":"Transportation of H2O and melting in subduction zones"}],"description":[{"notation":[{"@value":"Abstract   Material recycling in subduction zones, including the generation and migration of aqueous fluids and melts, is key to understanding the origin of volcanism in subduction zones and is also important for understanding the global circulation of materials. Recent knowledge concerning the phase relationships of hydrous peridotitic and basaltic systems allows us to model the fluid generation and migration in subduction zones. Here I present a numerical model, in which the aqueous fluid migrates by permeable flow and interacts chemically with the convecting solid, including melting. The calculation results suggest that nearly all the H2O expelled from the subducting slab will be hosted by serpentine and chlorite just above the slab, and is brought down by up to 150 km, depending on the temperature along the slab. Breakdown of serpentine and chlorite at these depths results in the formation of a fluid column through which H2O is transported upwards. The fluid reaches a depth corresponding to a cusp of the H2O-undersaturated solidus of peridotite (minimum at 2.5 GPa) and initiates extensive melting whose depth and the lateral extent toward the trench side is nearly fixed, irrespective of the age of the slab. This is because the flux of H2O and the depression of the practical solidus temperature in the mantle wedge are similar for models with different slab ages. Exceptionally, for very young slabs (e.g. ≪10 Myr when the subduction velocity is ∼6 cm/y), different melting regimes occur, such as melting in the forearc region and slab melting. If the aqueous fluid released from the slab migrates upwards in disequilibrium (e.g. through fractures), significant melting occurs in the forearc region, since the serpentinite layer, an effective H2O-absorber, is not formed. However, this is not the case in most subduction zones. Further studies with various subduction parameters, and melt segregation processes which are not included in this study, are required to compare the model results with the observed distribution and chemistry of arc magmas."}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1381137045826553344","@type":"Researcher","foaf:name":[{"@value":"Hikaru Iwamori"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"0012821X"},{"@type":"PISSN","@value":"http://id.crossref.org/issn/0012821X"}],"prism:publicationName":[{"@value":"Earth and Planetary Science Letters"}],"dc:publisher":[{"@value":"Elsevier BV"}],"prism:publicationDate":"1998-07","prism:volume":"160","prism:number":"1-2","prism:startingPage":"65","prism:endingPage":"80"},"reviewed":"false","dc:rights":["https://www.elsevier.com/tdm/userlicense/1.0/"],"url":[{"@id":"https://api.elsevier.com/content/article/PII:S0012821X98000806?httpAccept=text/xml"},{"@id":"https://api.elsevier.com/content/article/PII:S0012821X98000806?httpAccept=text/plain"}],"createdAt":"2002-07-25","modifiedAt":"2019-04-24","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050013474495795840","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"A review on slow earthquakes in the Japan Trench"}]},{"@id":"https://cir.nii.ac.jp/crid/1050298975368397568","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"3D thermal structural and dehydration modeling in the southern Chile subduction zone and its relationship to interplate earthquakes and the volcanic chain"}]},{"@id":"https://cir.nii.ac.jp/crid/1050573243559206016","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Estimation of spatial distribution and fluid fraction of a potential supercritical geothermal reservoir by magnetotelluric data: a case study from Yuzawa geothermal field, NE Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1050860322104047360","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"3-D thermal structure and dehydration near the Chile Triple Junction and its relation to slab window, tectonic tremors, and volcanoes"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002214349850112","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Electrical image of subduction zone beneath northeastern Japan"}]},{"@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/1360004229803726080","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Temperature and melt fraction distributions in a mantle wedge determined from the electrical conductivity structure: Application to one nonvolcanic and two volcanic regions in the Kyushu subduction zone, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004229807600000","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Fluid Migration in a Subducting Viscoelastic 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