{"@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/1362825895285719552.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1111/jmg.12072"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fjmg.12072"}},{"identifier":{"@type":"URI","@value":"https://onlinelibrary.wiley.com/doi/pdf/10.1111/jmg.12072"}}],"dc:title":[{"@value":"Elasticity of lawsonite and seismological signature of metamorphism and water cycling in the subducting oceanic crust"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Abstract</jats:title><jats:p>The elastic properties of lawsonite determined from equations of state, Brillouin scattering, acoustic velocity measurements, and first‐principles calculations are reviewed. Equations of state are essential for thermodynamic modelling of phase equilibrium at high pressure. Elastic tensor determinations allow calculation of the seismic properties of isotropic rocks, and of anisotropic rocks when combined with <jats:styled-content style=\"fixed-case\">CPO</jats:styled-content> determinations. Potential effects of low‐<jats:italic>T</jats:italic>, high‐<jats:italic>P</jats:italic> phase transitions in lawsonite on extrapolations to deep‐Earth conditions are discussed. Seismological data suggest that metamorphic zoning in active cold subduction zones can be resolved as low velocity layers down to 250 km. Mineral physics and phase equilibria indicate that lawsonite is the best candidate for explaining such low velocities. These layers are likely the image of water recycling to the deep mantle in subduction zones.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380285711776172947","@type":"Researcher","foaf:name":[{"@value":"B. Reynard"}],"jpcoar:affiliationName":[{"@value":"Université de Lyon Lyon France"},{"@value":"CNRS Lyon France"},{"@value":"Ecole Normale Supérieure de Lyon Site Monod, 15 parvis René Descartes BP7000 F‐69342 Lyon France"},{"@value":"Université Claude Bernard Lyon 1 43 Bd du 11 Novembre 1918 F‐69622 Villeurbanne Cedex France"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825895285719552","@type":"Researcher","foaf:name":[{"@value":"J. D. Bass"}],"jpcoar:affiliationName":[{"@value":"Department of Geology University of Illinois Urbana IL 61801 USA"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"02634929"},{"@type":"EISSN","@value":"15251314"}],"prism:publicationName":[{"@value":"Journal of Metamorphic Geology"}],"dc:publisher":[{"@value":"Wiley"}],"prism:publicationDate":"2014-02-24","prism:volume":"32","prism:number":"5","prism:startingPage":"479","prism:endingPage":"487"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fjmg.12072"},{"@id":"https://onlinelibrary.wiley.com/doi/pdf/10.1111/jmg.12072"}],"createdAt":"2013-12-30","modifiedAt":"2023-09-11","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360004232523458176","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Seismic properties of lawsonite eclogites from the southern Motagua fault zone, Guatemala"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004235781788288","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Lawsonite blueschists and lawsonite eclogites as proxies for palaeo‐subduction zone processes: a review"}]},{"@id":"https://cir.nii.ac.jp/crid/1361694367058083328","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Experimentally deformed lawsonite at high pressure and high temperature: Implication for low velocity layers in subduction zones"}]},{"@id":"https://cir.nii.ac.jp/crid/2050025942186665344","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Guided wave observations and evidence for the low-velocity subducting crust beneath Hokkaido, northern Japan"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1111/jmg.12072"},{"@type":"CROSSREF","@value":"10.1111/jmg.12057_references_DOI_G8dO3o6xsXQQdMjxsbpJ5euz5QA"},{"@type":"CROSSREF","@value":"10.1186/1880-5981-66-69_references_DOI_G8dO3o6xsXQQdMjxsbpJ5euz5QA"},{"@type":"CROSSREF","@value":"10.1016/j.pepi.2019.106282_references_DOI_G8dO3o6xsXQQdMjxsbpJ5euz5QA"},{"@type":"CROSSREF","@value":"10.1016/j.tecto.2016.04.012_references_DOI_G8dO3o6xsXQQdMjxsbpJ5euz5QA"}]}