{"@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/1362262944731155072.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1007/s004100100263"}},{"identifier":{"@type":"URI","@value":"http://link.springer.com/content/pdf/10.1007/s004100100263.pdf"}},{"identifier":{"@type":"URI","@value":"http://link.springer.com/article/10.1007/s004100100263/fulltext.html"}},{"identifier":{"@type":"URI","@value":"http://link.springer.com/content/pdf/10.1007/s004100100263"}}],"dc:title":[{"@value":"Morphology of intergranular pores and wetting angles in pelitic schists studied by transmission electron microscopy"}],"description":[{"notation":[{"@value":"In pelitic schists composed mainly of quartz and albite grains, the morphology of intergranular pores, which were filled with water, was studied by transmission electron microscopy (TEM). Although some pores are defined by crystallographic planes (F-face), most of their form has an ideal shape determined by interface tensions between grains and fluid. High-resolution TEM observations demonstrate that pore-free regions at grain boundaries are tight even at the nanometer scale, showing that the wetting angle is larger than 0° in this rock. The pore distribution in two-grain junctions can be compared to a \"necklace microstructure\" developed by instability of a fluid film along the boundary induced by microcracking. Wetting angles for pores located at grain edges of quartz and albite decrease in the order albite/albite, quartz/quartz, and quartz/albite. The quartz/quartz wetting angle in a calcite-free sample is smaller than that in a calcite-containing sample. This angle also changes due to grain misorientation. Our results confirm that solid–solid and solid–fluid interfacial energies control the geometry of intergranular fluid in natural rocks."}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1382262944731155074","@type":"Researcher","foaf:name":[{"@value":"Takehiko Hiraga"}]},{"@id":"https://cir.nii.ac.jp/crid/1382262944731155075","@type":"Researcher","foaf:name":[{"@value":"Osamu Nishikawa"}]},{"@id":"https://cir.nii.ac.jp/crid/1382262944731155073","@type":"Researcher","foaf:name":[{"@value":"Toshiro Nagase"}]},{"@id":"https://cir.nii.ac.jp/crid/1382262944731155072","@type":"Researcher","foaf:name":[{"@value":"Mizuhiko Akizuki"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00107999"},{"@type":"EISSN","@value":"14320967"},{"@type":"PISSN","@value":"http://id.crossref.org/issn/00107999"},{"@type":"PISSN","@value":"https://id.crossref.org/issn/00107999"}],"prism:publicationName":[{"@value":"Contributions to Mineralogy and Petrology"}],"dc:publisher":[{"@value":"Springer Science and Business Media LLC"}],"prism:publicationDate":"2001-08","prism:volume":"141","prism:number":"5","prism:startingPage":"613","prism:endingPage":"622"},"reviewed":"false","dc:rights":["http://www.springer.com/tdm"],"url":[{"@id":"http://link.springer.com/content/pdf/10.1007/s004100100263.pdf"},{"@id":"http://link.springer.com/article/10.1007/s004100100263/fulltext.html"},{"@id":"http://link.springer.com/content/pdf/10.1007/s004100100263"}],"createdAt":"2010-10-01","modifiedAt":"2019-05-28","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/1360286990822610944","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Kinetics and duration of metamorphic mineral growth in a subduction complex: zircon and phengite in the Nagasaki metamorphic complex, western Kyushu, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360576118713913600","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Enhancement of ductile deformation in polycrystalline anorthite due to the addition of water"}]},{"@id":"https://cir.nii.ac.jp/crid/1360584340506182912","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Porosity generation via spatially uncoupled dissolution precipitation during plagioclase replacement in quartz undersaturated fluids"}]},{"@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"],"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/1390001206545736448","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Water at high temperatures in a microcrystalline silica (chalcedony) by in-situ infrared spectroscopy: physicochemical states and dehydration behavior"},{"@value":"Water at high temperatures in microcrystalline silica (chalcedony) by in situ infrared spectroscopy: physicochemical states and dehydration behavior"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1007/s004100100263"},{"@type":"OPENAIRE","@value":"doi_dedup___::efe679f69d25fc2107a41ae920432ba6"},{"@type":"CROSSREF","@value":"10.1007/s00410-019-1629-8_references_DOI_73BqnUzB3mx3FELUkLMwGa8PXxA"},{"@type":"CROSSREF","@value":"10.2465/gkk.39.101018_references_DOI_73BqnUzB3mx3FELUkLMwGa8PXxA"},{"@type":"CROSSREF","@value":"10.5575/geosoc.2017.0009_references_DOI_73BqnUzB3mx3FELUkLMwGa8PXxA"},{"@type":"CROSSREF","@value":"10.1016/j.jsg.2022.104547_references_DOI_73BqnUzB3mx3FELUkLMwGa8PXxA"},{"@type":"CROSSREF","@value":"10.1007/s00410-023-02088-8_references_DOI_73BqnUzB3mx3FELUkLMwGa8PXxA"},{"@type":"CROSSREF","@value":"10.1186/s40623-019-1117-4_references_DOI_73BqnUzB3mx3FELUkLMwGa8PXxA"},{"@type":"CROSSREF","@value":"10.2465/jmps.071022a_references_DOI_73BqnUzB3mx3FELUkLMwGa8PXxA"}]}