{"@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/1360574096410067968.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1016/0040-1951(81)90089-5"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:0040195181900895?httpAccept=text/xml"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:0040195181900895?httpAccept=text/plain"}}],"dc:title":[{"@value":"Microstructural development of fine-grained quartz aggregates by syntectonic recrystallization"}],"description":[{"notation":[{"@value":"Abstract   Experimental study of syntectonic recrystallization of fine-grained quartz aggregates was carried out in order to simulate the development of some natural microstructures of quartz tectonites and to understand their formation condition. Agate was axially compressed with a constant-strain-rate apparatus. Experiments were conducted at 4 kbar solid confining pressure, 700–1000°C and 10 −4 -10 −6  sec −1  to 10%–45% strain. In all runs, deformation has proceeded under wet condition caused by dehydration of pyrophyllite used as pressure medium.  Two different types of microstructure were distinguished in the deformed specimens. One is P-type which is characterized by equant, equidimensional, and polygonal grains. The other is S-type which is characterized by the highly oblate grains with the largest dimension perpendicular to the compression axis. The P-type microstructure is developed at higher temperatures and slower strain rates, while the S-type developed at lower temperatures and faster strain rates. The transition between the S- and P-types is found to be very sharp."}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380574096410067969","@type":"Researcher","foaf:name":[{"@value":"Toshiaki Masuda"}]},{"@id":"https://cir.nii.ac.jp/crid/1380574096410067968","@type":"Researcher","foaf:name":[{"@value":"Akio Fujimura"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00401951"}],"prism:publicationName":[{"@value":"Tectonophysics"}],"dc:publisher":[{"@value":"Elsevier BV"}],"prism:publicationDate":"1981-01","prism:volume":"72","prism:number":"1-2","prism:startingPage":"105","prism:endingPage":"128"},"reviewed":"false","dc:rights":["https://www.elsevier.com/tdm/userlicense/1.0/"],"url":[{"@id":"https://api.elsevier.com/content/article/PII:0040195181900895?httpAccept=text/xml"},{"@id":"https://api.elsevier.com/content/article/PII:0040195181900895?httpAccept=text/plain"}],"createdAt":"2003-08-07","modifiedAt":"2019-03-15","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/1360004232324909440","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Integrated estimates of the thickness of the fault damage zone in granitic terrain based on penetrative mesocracks and XRD analyses of quartz"}]},{"@id":"https://cir.nii.ac.jp/crid/1360016864725504128","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Steady-State Microstructures of Quartz Revisited: Evaluation of Stress States in Deformation Experiments Using a Solid-Medium Apparatus"}]},{"@id":"https://cir.nii.ac.jp/crid/1360283690266681856","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Grain growth kinetics and the effect of crystallographic anisotropy on normal grain growth of quartz"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206238726528","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Petrology and radiogenic age of accidental clasts of granitic mylonite from the Aso-4 pyroclastic flow deposit and their correlation to the Nioki Granite"},{"@language":"ja","@value":"Aso-4火砕流堆積物中の花崗岩マイロナイト異質礫の岩石学と放射年代および荷尾杵花崗岩との対比"},{"@language":"ja-Kana","@value":"Aso 4 カサイリュウ タイセキブツ チュウ ノ カコウガン マイロナイト イシツレキ ノ ガンセキガク ト ホウシャ ネンダイ オヨビ ニオキ カコウガン ト ノ タイヒ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206240772480","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Mylonitization of older dikes in the Ryoke Belt, Awaji Island, SW Japan"},{"@language":"ja","@value":"淡路島の領家帯古期岩脈のマイロナイト化作用"},{"@language":"ja-Kana","@value":"アワジシマ ノ リョウケタイ コキガン ミャク ノ マイロナイトカ サヨウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681490857344","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Heterogeneous material distribution, an important reason for generation of strain-localized mylonite and frictional slip zones in the Hidaka metamorphic belt, Hokkaido, Japan"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1016/0040-1951(81)90089-5"},{"@type":"OPENAIRE","@value":"doi_dedup___::11230f3f6b08305c6c58d34a9d4da01d"},{"@type":"CROSSREF","@value":"10.5575/geosoc.113.1_references_DOI_8wieSZxLnB1uqo9mVc5PyNUYuY8"},{"@type":"CROSSREF","@value":"10.3390/min12030329_references_DOI_8wieSZxLnB1uqo9mVc5PyNUYuY8"},{"@type":"CROSSREF","@value":"10.1007/s00269-011-0476-6_references_DOI_8wieSZxLnB1uqo9mVc5PyNUYuY8"},{"@type":"CROSSREF","@value":"10.1016/j.jsg.2011.11.008_references_DOI_8wieSZxLnB1uqo9mVc5PyNUYuY8"},{"@type":"CROSSREF","@value":"10.1186/bf03353344_references_DOI_8wieSZxLnB1uqo9mVc5PyNUYuY8"},{"@type":"CROSSREF","@value":"10.5575/geosoc.2013.0054_references_DOI_8wieSZxLnB1uqo9mVc5PyNUYuY8"},{"@type":"CROSSREF","@value":"10.1186/s40623-019-1117-4_references_DOI_8wieSZxLnB1uqo9mVc5PyNUYuY8"}]}