{"@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/1363670320090289152.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/93gl01382"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F93GL01382"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/93GL01382"}}],"dc:title":[{"@value":"Relationships between dynamically recrystallized grain size and deformation conditions in experimentally deformed olivine rocks"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>New microstructural data on experimentally deformed “wet” and “dry” natural olivine rocks (Anita Bay and Åheim dunite), together with the other reliable experimental data, indicate that the experimental stress‐recrystallized grain size relationship in olivine‐rocks is largely independent of water content and temperature, and is only slightly dependent on the flow properties of the material. The experimental data cover a stress range of 30–300 MPa, water contents from <30 ppm to 300 ppm, and temperatures in the range 1100–1650°C. Local melt contents of up to 10 volume% cannot be demonstrated to have a significant effect on the stress—grain size relationship.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1383670320090289154","@type":"Researcher","foaf:name":[{"@value":"Dirk Van der Wal"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670320090289024","@type":"Researcher","foaf:name":[{"@value":"Prame Chopra"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670320090289153","@type":"Researcher","foaf:name":[{"@value":"Martyn Drury"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670320090289152","@type":"Researcher","foaf:name":[{"@value":"John Fitz Gerald"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00948276"},{"@type":"EISSN","@value":"19448007"}],"prism:publicationName":[{"@value":"Geophysical Research Letters"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"1993-07-23","prism:volume":"20","prism:number":"14","prism:startingPage":"1479","prism:endingPage":"1482"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F93GL01382"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/93GL01382"}],"createdAt":"2008-02-06","modifiedAt":"2023-11-22","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050845763798672128","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Rheological contrast between garnet and clinopyroxene in the mantle wedge : An example from Higashi-akaishi peridotite mass, SW Japan"},{"@value":"Rheological contrast between garnet and clinopyroxene in the mantle wedge: an example from Higashi-akaishi peridotite mass"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002215916231936","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Olivine fabric evolution in a hydrated ductile shear zone at the Moho Transition Zone, Oman Ophiolite"}]},{"@id":"https://cir.nii.ac.jp/crid/1360025429411606656","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Deformation and melt–rock interaction in the upper mantle: Insights from the layered structure of the Horoman peridotite, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285704785187968","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Rheological Weakening of Olivine + Orthopyroxene Aggregates Due to Phase Mixing: 1. 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