{"@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/1360002216044668672.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1016/j.jsg.2011.10.004"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0191814111001660?httpAccept=text/xml"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0191814111001660?httpAccept=text/plain"}}],"resourceType":"学術雑誌論文(journal article)","dc:title":[{"@value":"Textures of syntaxial quartz veins synthesized by hydrothermal experiments"}],"description":[{"notation":[{"@value":"Syntaxial quartz veins were synthesized by hydrothermal flow-through experiments using rock blocks (metachert, sandstone, and granite) containing slits. Based on analyses of vein textures using birefringence imaging microscopy, we identified two stages of crystal growth. During stage 1, quartz grain growth occurs without an increase in grain width. During stage 2, quartz grains develop facets and grow preferentially parallel to the c-axis orientation, and the aspect ratio of quartz grains shifts toward ∼2.9. Competitive growth occurs significantly at stage 2, and the transition from stage 1–2 occurs at a critical distance from the vein wall, being approximately equal to the host-rock grain size. Crystal growth in the slits produce various textures controlled by the ratio of slit aperture (H) to host-rock grain size (d). In high H/d cracks, elongate–blocky texture develops by grain impingement during stage 2, whereas in low H/d cracks, crystals that bridge the crack form without competitive growth by grain impingement at stage 1. Heterogeneous structures of fracture porosity are produced during syntaxial vein formation, due to the anisotropy in the growth rate of quartz. Such “incompletely sealed” cracks may act as important fluid pathways and as weak planes in the upper crust."}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1420564276185137408","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"40422092"},{"@type":"NRID","@value":"1000040422092"},{"@type":"ORCID","@value":"0000-0001-5757-6279"},{"@type":"NRID","@value":"9000004619111"},{"@type":"NRID","@value":"9000406036489"},{"@type":"NRID","@value":"9000007392263"},{"@type":"NRID","@value":"9000331910094"},{"@type":"NRID","@value":"9000014352329"},{"@type":"NRID","@value":"9000016866067"},{"@type":"NRID","@value":"9000347083272"},{"@type":"NRID","@value":"9000007144483"},{"@type":"NRID","@value":"9000242709943"},{"@type":"NRID","@value":"9000001757151"},{"@type":"NRID","@value":"9000015509619"},{"@type":"NRID","@value":"9000401431767"},{"@type":"NRID","@value":"9000283245939"},{"@type":"NRID","@value":"9000406039061"},{"@type":"NRID","@value":"9000361706723"},{"@type":"NRID","@value":"9000243767062"},{"@type":"NRID","@value":"9000242718760"},{"@type":"NRID","@value":"9000257917426"},{"@type":"NRID","@value":"9000007741651"},{"@type":"NRID","@value":"9000018889430"},{"@type":"NRID","@value":"9000019149861"},{"@type":"NRID","@value":"9000004606180"},{"@type":"NRID","@value":"9000024320646"},{"@type":"NRID","@value":"9000350560113"},{"@type":"NRID","@value":"9000258410810"},{"@type":"NRID","@value":"9000403552226"},{"@type":"NRID","@value":"9000406038164"},{"@type":"NRID","@value":"9000009652210"},{"@type":"NRID","@value":"9000009316132"},{"@type":"NRID","@value":"9000241476495"},{"@type":"NRID","@value":"9000017737831"},{"@type":"NRID","@value":"9000242078426"},{"@type":"NRID","@value":"9000413779496"},{"@type":"NRID","@value":"9000332226141"},{"@type":"NRID","@value":"9000399529083"},{"@type":"NRID","@value":"9000319553385"},{"@type":"NRID","@value":"9000350559714"},{"@type":"NRID","@value":"9000258410347"},{"@type":"NRID","@value":"9000342792786"},{"@type":"NRID","@value":"9000254824586"},{"@type":"NRID","@value":"9000403550694"},{"@type":"NRID","@value":"9000406038270"},{"@type":"NRID","@value":"9000258410555"},{"@type":"NRID","@value":"9000412653224"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/winchite"}],"foaf:name":[{"@value":"Atsushi Okamoto"}]},{"@id":"https://cir.nii.ac.jp/crid/1380847869148616321","@type":"Researcher","foaf:name":[{"@value":"Kotaro Sekine"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"01918141"}],"prism:publicationName":[{"@value":"Journal of Structural Geology"}],"dc:publisher":[{"@value":"Elsevier BV"}],"prism:publicationDate":"2011-12","prism:volume":"33","prism:number":"12","prism:startingPage":"1764","prism:endingPage":"1775"},"reviewed":"false","dc:rights":["https://www.elsevier.com/tdm/userlicense/1.0/","https://www.elsevier.com/legal/tdmrep-license"],"url":[{"@id":"https://api.elsevier.com/content/article/PII:S0191814111001660?httpAccept=text/xml"},{"@id":"https://api.elsevier.com/content/article/PII:S0191814111001660?httpAccept=text/plain"}],"createdAt":"2011-10-17","modifiedAt":"2025-10-01","project":[{"@id":"https://cir.nii.ac.jp/crid/1040282257078686720","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"22109501"},{"@type":"JGN","@value":"JP22109501"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PUBLICLY-22109501/"}],"notation":[{"@language":"ja","@value":"沈み込み帯浅部における流体移動と水―岩石相互作用に関する実験的研究"}]},{"@id":"https://cir.nii.ac.jp/crid/1040282257150898048","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"23654180"},{"@type":"JGN","@value":"JP23654180"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-23654180/"}],"notation":[{"@language":"ja","@value":"鉱物・流体包有物形成における分別作用:岩石形成過程への新アプローチ"},{"@language":"en","@value":"Fractionation during formation of mineral/fluid inclusions: A new approach for understanding of rock-forming processes"}]}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050001202731768320","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Velocity of vertical fluid ascent within vein-forming fractures"}]},{"@id":"https://cir.nii.ac.jp/crid/1050001202731779200","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Determination of aperture structure and fluid flow in a rock fracture by a high-resolution numerical modeling on the basis of a flow-through experiment under confining pressure"}]},{"@id":"https://cir.nii.ac.jp/crid/1050001338868541824","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Grain-size-sensitive deformation of upper greenschist- to lower 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