{"@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/1361699996188855424.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1111/j.1525-1314.1998.00060.x"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1525-1314.1998.00060.x"}},{"identifier":{"@type":"URI","@value":"https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1525-1314.1998.00060.x"}}],"dc:title":[{"@value":"Progressive sequence of reactions of the Ryoke metamorphism in the Yanai district, southwest Japan: the formation of cordierite"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>The compositions of biotite and muscovite were examined in terms of the paragenesis and the metamorphic grade in low‐ to medium‐grade pelitic rocks of the Ryoke metamorphism in the Yanai district, southwest Japan. The biotite and muscovite that coexist with K‐feldspar have a higher K component in an A′KF diagram than those in rocks lacking K‐feldspar. This fact reflects an increase in the K<jats:sub>2</jats:sub>O content in muscovite, but in biotite it reflects an increase of not only the K<jats:sub>2</jats:sub>O content but also of the octahedral vacancy.</jats:p><jats:p>At higher metamorphic grade beyond the cordierite isograd, where cordierite coexists with neither chlorite nor K‐feldspar, the biotite shows an increase in illite, K Aliv □xii−1 Si−1, and Tschermak components, Alvi Aliv R+−1 Si−1, where □xii and R+ denote the interlayer vacancy and (Fe+Mg+Mn), respectively. A reaction to define the cordierite isograd is proposed by treating this chemical change as being responsible for the first appearance of cordierite, i.e. K,Al‐poor biotite+phengitic muscovite=K,Al‐rich biotite+cordierite+quartz+water .By treating this as a key reaction in medium‐grade metamorphism, a set of reaction in a progressive metamorphism is established for the Ryoke metamorphism, a typical low‐pressure type metamorphism. Some textures in one of the high‐grade areas, the K‐feldspar‐cordierite zone, suggest that a further two prograde reactions have taken place, i.e. andalusite+biotite+quartz=cordierite+K‐feldspar+water</jats:p><jats:p>and  andalusite=sillimanite.quartz=cordierite+K‐feldspar+water</jats:p><jats:p>This implies that this zone probably has a P–T  path involving isobaric heating.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380848656160332165","@type":"Researcher","foaf:name":[{"@value":"T. IKEDA"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"02634929"},{"@type":"EISSN","@value":"15251314"},{"@type":"PISSN","@value":"https://id.crossref.org/issn/02634929"}],"prism:publicationName":[{"@value":"Journal of Metamorphic Geology"}],"dc:publisher":[{"@value":"Wiley"}],"prism:publicationDate":"1998-01","prism:volume":"16","prism:number":"1","prism:startingPage":"39","prism:endingPage":"52"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1525-1314.1998.00060.x"},{"@id":"https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1525-1314.1998.00060.x"}],"createdAt":"2004-10-08","modifiedAt":"2023-09-11","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050001338855258496","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Disequilibrium REE compositions of garnet and zircon in migmatites reflecting different growth timings during single metamorphism (Aoyama area, Ryoke belt, Japan)"}]},{"@id":"https://cir.nii.ac.jp/crid/1050282810743826432","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Behavior of zircon in the upper-amphibolite to granulite facies schist/migmatite transition, Ryoke metamorphic belt, SW Japan: constraints from the melt inclusions in zircon"}]},{"@id":"https://cir.nii.ac.jp/crid/1050845760787672832","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Spatiotemporal evolution of magmatic pulses and regional metamorphism during a Cretaceous flare-up event: Constraints from the Ryoke belt (Mikawa area, central 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カテイ"},{"@value":"Emplacement process of the Hatsuse plutonic complex, central Kinki Province,"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206239362944","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"K–Ar ages of the Ryoke plutonic rocks in the Asuke area, Aichi prefecture, central Japan"},{"@language":"ja","@value":"中部地方領家帯，足助地域に分布する深成岩類のK–Ar年代"},{"@language":"ja-Kana","@value":"チュウブ チホウ リョウケタイ,アシ ジョ チイキ ニ ブンプ スル シンセイガンルイ ノ K-Ar ネンダイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206239966208","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"K-Ar ages of low-grade metapelites from the Ryoke belt, the Iwakuni district, Yamaguchi Prefecture, Japan"},{"@language":"ja","@value":"山口県東部，岩国地域領家帯低度変成岩の白雲母K-Ar年代"},{"@language":"ja-Kana","@value":"ヤマグチケン トウブ,イワクニ チイキ リョウケタイ テイド ヘンセイガン ノ ハクウンモ K-Ar 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アプローチ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390008078423674496","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Igneous and metamorphic rocks in Kasuga region, western Gifu Prefecture, Japan"},{"@language":"ja","@value":"岐阜県西部・揖斐川町春日地域の火成岩と接触変成岩"},{"@language":"ja-Kana","@value":"ギフケン セイブ ・ イビガワマチ カスガ チイキ ノ カセイガン ト セッショク ヘンセイガン"}]},{"@id":"https://cir.nii.ac.jp/crid/1390013474494716288","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Terminology of “potassium feldspar” and “alkali feldspar”"},{"@language":"ja","@value":"用語「カリ長石」と「アルカリ長石」について"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679205666048","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Cretaceous Events at the Eastern Margin of East Asia Recorded in Rocks of the Ryoke Belt, SW Japan"},{"@language":"ja","@value":"領家帯に記録された東アジア東縁の白亜紀イベント"},{"@language":"ja-Kana","@value":"リョウケタイ ニ キロク サレタ ヒガシアジア トウエン ノ ハクアキ イベント"},{"@value":"Cretaceous events at the eastern margin of the East Asia recorded in rocks of the Ryoke belt,"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681214525312","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Decompressional microstructure from garnet-bearing mafic granulite in Yanai district, Ryoke belt, Southwest Japan"},{"@language":"ja","@value":"領家帯柳井地域の含ざくろ石苦鉄質グラニュライトから見出された減圧組織"},{"@language":"ja-Kana","@value":"リョウケタイ ヤナイ チイキ ノ ガンザクロセキ クテツシツ グラニュライト カラ ミイダサレタ ゲンアツ ソシキ"},{"@language":"ja-Kana","@value":"リョウケタイ ヤナイ チイキ ノ ガンザクロイシクテツシツ グラニュライト カラ ミイダサレタ ゲンアツ ソシキ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681216947584","@type":"Article","resourceType":"学術雑誌論文(journal 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article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Large thermal aureole around the Inagawa Granodiorite in the southeastern area of Asuke, Aichi Prefecture"},{"@language":"ja","@value":"愛知県足助南東部地域における伊奈川花崗閃緑岩の広大な接触変成帯"},{"@language":"ja-Kana","@value":"アイチケン ソク ジョ ナントウブ チイキ ニ オケル イナガワ ハナオカセンリョクガン ノ コウダイ ナ セッショク ヘンセイタイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681522244992","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Geology and metamorphic zonation of the Ryoke Metamorphic Belt on Kasado-jima Island, SW Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282763121133568","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Magma process of Gamano granodiorite in Ryoke belt, Yanai region, Yamaguchi, Southwest 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