{"@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/1361418520795556352.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1144/gsl.sp.2005.245.01.19"}},{"identifier":{"@type":"URI","@value":"https://www.lyellcollection.org/doi/pdf/10.1144/GSL.SP.2005.245.01.19"}}],"dc:title":[{"@value":"Water distribution in dynamically recrystallized quartz grains: cathodoluminescence and micro-infrared spectroscopic mapping"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Abstract</jats:title>\n          <jats:p>\n            The distribution of water in dynamically recrystallized quartz aggregates in granitic mylonites was investigated by cathodoluminescence (CL) observations and micro-infrared (IR) spectroscopic mapping. It is clear from CL observations and micro-IR spectroscopic mappings that the CL intensity and contrast depend on the density of defects (e.g. the content of molecular H\n            <jats:sub>2</jats:sub>\n            O and absorbed OH species). Dynamic recrystallization, as a recovery process of intracrystalline strain, decreases the densities of excess carriers originated from defects. The decrease in the densities of excess carriers decreases the CL intensity and contrast within each grain. To investigate the effect of water weakening in the rheological properties of the crust, CL spectroscopy and micro-IR spectroscopic mapping are essential in the determination of concentration and distribution of water in natural high-strain zones.\n          </jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1381418520795556353","@type":"Researcher","foaf:name":[{"@value":"Jun Muto"}],"jpcoar:affiliationName":[{"@value":"Department of Geoenvironmental Sciences, Graduate School of Science, Tohoku University\rAoba-ku, Sendai 980-8578, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1381418520795556352","@type":"Researcher","foaf:name":[{"@value":"Hiroyuki Nagahama"}],"jpcoar:affiliationName":[{"@value":"Department of Geoenvironmental Sciences, Graduate School of Science, Tohoku University\rAoba-ku, Sendai 980-8578, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1381418520795556354","@type":"Researcher","foaf:name":[{"@value":"Testsuo Hashimoto"}],"jpcoar:affiliationName":[{"@value":"Department of Chemistry, Faculty of Science, Niigata University\rIkarashi-Ninocho, Niigata 950-2181, Japan"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"03058719"},{"@type":"EISSN","@value":"20414927"}],"prism:publicationName":[{"@value":"Geological Society, London, Special Publications"}],"dc:publisher":[{"@value":"Geological Society of London"}],"prism:publicationDate":"2005-01","prism:volume":"245","prism:number":"1","prism:startingPage":"397","prism:endingPage":"407"},"reviewed":"false","dc:rights":["https://doi.org/10.15223/policy-002"],"url":[{"@id":"https://www.lyellcollection.org/doi/pdf/10.1144/GSL.SP.2005.245.01.19"}],"createdAt":"2008-04-30","modifiedAt":"2024-07-24","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050012570392438528","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Water distribution in quartz schists of the Sanbagawa Metamorphic Belt, Japan: infrared spectroscopic mapping and comparison of the calibrations proposed for determining water contents"}]},{"@id":"https://cir.nii.ac.jp/crid/1360580229804889600","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Water release and homogenization by dynamic recrystallization of quartz"}]},{"@id":"https://cir.nii.ac.jp/crid/1390301330606010752","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Exploring the Eastern Abukuma Mountains: A field guide to high-pressure metamorphic rocks and strike-slip crustal shear zones in the Southern Kitakami Belt, NE Japan"},{"@language":"ja","@value":"阿武隈山地東縁を探る：南部北上帯の高圧型片岩類と横ずれ剪断帯のフィールドガイド"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1144/gsl.sp.2005.245.01.19"},{"@type":"OPENAIRE","@value":"doi_dedup___::f97dd2f7302b008419eac219527a04fe"},{"@type":"CROSSREF","@value":"10.5194/se-14-409-2023_references_DOI_VrE9OCb9Xt5bJNqYzhntcWzPAdB"},{"@type":"CROSSREF","@value":"10.5575/geosoc.2024.0022_references_DOI_VrE9OCb9Xt5bJNqYzhntcWzPAdB"},{"@type":"CROSSREF","@value":"10.1186/s40623-019-1117-4_references_DOI_VrE9OCb9Xt5bJNqYzhntcWzPAdB"}]}