{"@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/1363670318443841536.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1007/s002690050226"}},{"identifier":{"@type":"URI","@value":"http://link.springer.com/content/pdf/10.1007/s002690050226.pdf"}},{"identifier":{"@type":"URI","@value":"http://link.springer.com/article/10.1007/s002690050226/fulltext.html"}},{"identifier":{"@type":"URI","@value":"http://link.springer.com/content/pdf/10.1007/s002690050226"}},{"identifier":{"@type":"NAID","@value":"80011340627"}}],"dc:title":[{"@value":"The structure of grain boundaries in granite-origin ultramylonite studied by high-resolution electron microscopy"}],"description":[{"notation":[{"@value":"The structure of grain boundaries in a granite-origin ultramylonite, composed mainly of fine-grained feldspar and quartz, was studied by high-resolution electron microscopy (HREM). At most of the boundaries, not only between the same minerals but also between different minerals, lattice fringes in adjacent grains meet at the interface with no other appreciable phases. In these boundaries, some of the straight segments correspond to a low-index plane of one of the connected grains. Boundaries containing voids, with a spheroidal shape elongated along the boundaries, were observed only between quartz grains. It is suggested that these boundaries were formed by healing of microcracks. The structural width of major boundaries, deduced from lattice-fringe imaging, is less than about 0.5 nm."}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1581135651714717696","@type":"Researcher","foaf:name":[{"@value":"T. Hiraga"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670318443841537","@type":"Researcher","foaf:name":[{"@value":"T. Nagase"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670318443841538","@type":"Researcher","foaf:name":[{"@value":"M. Akizuki"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"03421791"},{"@type":"EISSN","@value":"14322021"}],"prism:publicationName":[{"@value":"Physics and Chemistry of Minerals"}],"dc:publisher":[{"@value":"Springer Science and Business Media LLC"}],"prism:publicationDate":"1999-09-29","prism:volume":"26","prism:number":"8","prism:startingPage":"617","prism:endingPage":"623"},"reviewed":"false","dc:rights":["http://www.springer.com/tdm"],"url":[{"@id":"http://link.springer.com/content/pdf/10.1007/s002690050226.pdf"},{"@id":"http://link.springer.com/article/10.1007/s002690050226/fulltext.html"},{"@id":"http://link.springer.com/content/pdf/10.1007/s002690050226"}],"createdAt":"2002-08-25","modifiedAt":"2019-05-24","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/1360004229808443264","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Grain‐ to multiple‐grain‐scale deformation processes during diffusion creep of forsterite + diopside aggregate: 1. 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Grain boundary sliding‐induced grain rotation and its role in crystallographic preferred orientation in rocks"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848658349913216","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Olivine crystals align during diffusion creep of Earth’s upper mantle"}]},{"@id":"https://cir.nii.ac.jp/crid/1360861707120263168","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Diffusion Creep Characteristics of Anorthite Revealed by Uniaxial and Pure Shear Deformation Experiments"}]},{"@id":"https://cir.nii.ac.jp/crid/1360861707375192320","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Slab-derived fluid storage in the crust elucidated by earthquake swarm"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206239469568","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Rocks and advanced ceramics"},{"@language":"ja","@value":"岩石 vs ファインセラミックス"},{"@language":"ja-Kana","@value":"ガンセキ vs ファインセラミックス"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206526343680","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy","isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Connectivity of H2O fluids at depth: Insights from the thermodynamics of interfacial energy"},{"@language":"ja","@value":"深部　Ｈ２Ｏ　流体の連結性と界面の熱力学"},{"@language":"ja-Kana","@value":"シンブ H2O リュウタイ ノ レンケツセイ ト カイメン ノ ネツリキガク"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679064461568","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"The Structure of Grain Boundaries in Rocks Studied by High-Resolution Electron Microscopy."},{"@value":"高分解能電子顕微鏡で見た岩石の粒界構造"},{"@language":"ja-Kana","@value":"サイキン ノ ケンキュウ カラ コウ ブンカイノウ デンシ ケンビキョウ デ ミタ ガンセキ ノ リュウカイ コウゾウ"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1007/s002690050226"},{"@type":"CIA","@value":"80011340627"},{"@type":"OPENAIRE","@value":"doi_dedup___::8c53e2958340329e698fdb3bf6a044ab"},{"@type":"CROSSREF","@value":"10.1002/2017jb014254_references_DOI_KnXZgAJdZTiXjiCyrMwsCpJPR29"},{"@type":"CROSSREF","@value":"10.1029/2020jb019416_references_DOI_KnXZgAJdZTiXjiCyrMwsCpJPR29"},{"@type":"CROSSREF","@value":"10.5194/se-14-409-2023_references_DOI_KnXZgAJdZTiXjiCyrMwsCpJPR29"},{"@type":"CROSSREF","@value":"10.2465/gkk.39.101018_references_DOI_KnXZgAJdZTiXjiCyrMwsCpJPR29"},{"@type":"CROSSREF","@value":"10.5575/geosoc.2017.0009_references_DOI_KnXZgAJdZTiXjiCyrMwsCpJPR29"},{"@type":"CROSSREF","@value":"10.1002/2017jb014255_references_DOI_KnXZgAJdZTiXjiCyrMwsCpJPR29"},{"@type":"CROSSREF","@value":"10.1038/nature12570_references_DOI_KnXZgAJdZTiXjiCyrMwsCpJPR29"},{"@type":"CROSSREF","@value":"10.1029/2022jb024752_references_DOI_KnXZgAJdZTiXjiCyrMwsCpJPR29"},{"@type":"CROSSREF","@value":"10.1038/s43247-022-00610-7_references_DOI_KnXZgAJdZTiXjiCyrMwsCpJPR29"},{"@type":"CROSSREF","@value":"10.1186/s40623-019-1117-4_references_DOI_KnXZgAJdZTiXjiCyrMwsCpJPR29"}]}