{"@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/1363670319947312640.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1016/0012-821x(94)90117-1"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:0012821X94901171?httpAccept=text/xml"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:0012821X94901171?httpAccept=text/plain"}}],"dc:title":[{"@value":"Subduction of continental crust and terrigenous and pelagic sediments: an experimental study"}],"description":[{"notation":[{"@value":"Abstract   An important role for the recycling of terrigenous sediments in the mantle was proposed by Armstrong [1,2]. Aspects of this hypothesis have been tested via an experimental study of phase equilibria in a composition similar to that of average upper continental crust, over the pressure interval 6–24 GPa. This composition is sufficiently close to those of the principal argillaceous and siliceous classes of pelagic sediments to use the results to interpret the behaviour of these latter sediments, in addition to terrigenous sediments, during subduction. The subsolidus phase relationships displayed by lithologies derived from these materials are complex, with major roles being played by K-hollandite, garnet, Na-clinopyroxene and stishovite. Continentally derived lithologies achieve densities similar to, or greater than, surrounding mantle at depths greater than 200 km. The geodynamical implications of these buoyancy relationships are discussed.  A reconnaissance study has also been made to assess the melting and element partitioning behaviours in the subducted continental crust lithologies. During partial melting at relatively low pressures (5–10 GPa), orthoclase, wadeite and K-hollandite are eliminated near the solidus, whereas the stability field of Na-clinopyroxene extends to temperatures well above the solidus. Liquids formed by small to moderate degrees of partial melting of subducted, continentally derived lithologies in this pressure interval have high    K  Na    ratios and high SiO2 contents. At higher pressures (16–24 GPa), the stability fields of K-hollandite and stishovite extend towards the liquidus, whereas sodium-bearing phases are eliminated much closer to the solidus. Resultant partial melts consequently possess relatively low    K  Na    ratios and SiO2 contents. Lead possesses a high crystal-liquid partition coefficient in K-hollandite, whereas uranium is excluded. The broad stability field of K-hollandite during partial melting of these lithologies at pressures above 15 GPa therefore has the capacity to cause fractionation of lead from uranium. The petrological and geochemical implications of these results are discussed in the context of the partial melting of terrigenous materials during subduction and the interactions of the partial melts with the surrounding mantle."}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380004231198607618","@type":"Researcher","foaf:name":[{"@value":"T. Irifune"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670319947312642","@type":"Researcher","foaf:name":[{"@value":"A.E. Ringwood"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670319947312641","@type":"Researcher","foaf:name":[{"@value":"W.O. Hibberson"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"0012821X"}],"prism:publicationName":[{"@value":"Earth and Planetary Science Letters"}],"dc:publisher":[{"@value":"Elsevier BV"}],"prism:publicationDate":"1994-09","prism:volume":"126","prism:number":"4","prism:startingPage":"351","prism:endingPage":"368"},"reviewed":"false","dc:rights":["https://www.elsevier.com/tdm/userlicense/1.0/"],"url":[{"@id":"https://api.elsevier.com/content/article/PII:0012821X94901171?httpAccept=text/xml"},{"@id":"https://api.elsevier.com/content/article/PII:0012821X94901171?httpAccept=text/plain"}],"createdAt":"2002-11-11","modifiedAt":"2019-04-03","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050019900050053248","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Post-spinel-type AB2O4 high-pressure phases in geochemistry and materials 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Diamonds"}]},{"@id":"https://cir.nii.ac.jp/crid/1364227868969768448","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Thermoelastic Properties of K0.7Na0.3AlSi3O8 Hollandite and NaAlSi2O6 Jadeite: Implication for the Fate of the Subducted Continental Crust in the Deep Mantle"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204230813184","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Tectonic Erosion: New Perspectives on Pacific-type Orogeny and Continental Growth Models"},{"@language":"ja","@value":"構造浸食作用―太平洋型造山運動論と大陸成長モデルへの新視点―"},{"@language":"ja-Kana","@value":"コウゾウ シンショク サヨウ タイヘイヨウガタ ゾウザン ウンドウロン ト タイリク セイチョウ モデル エ ノ シン シテン"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204230827776","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"The Second Continent"},{"@language":"ja","@value":"第２大陸"},{"@language":"ja-Kana","@value":"ダイ2 タイリク"},{"@value":"The second continent (in Japanese with English abstract)"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204381265408","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"高圧実験と熱測定による地球内部物質の相転移および高圧結晶化学に関する研究"},{"@language":"en","@value":"Phase-Transition Studies on Earth's Materials by High-Pressure Experiments and Calorimetry, and Crystal-Chemical Studies on High-Pressure Inorganic Compounds"},{"@value":"受賞記念解説 高圧力学会学会賞 高圧実験と熱測定による地球内部物質の相転移および高圧結晶化学に関する研究"},{"@language":"ja-Kana","@value":"ジュショウ キネン カイセツ コウアツリョク ガッカイ ガッカイショウ コウアツ ジッケン ト ネツ ソクテイ ニ ヨル チキュウ ナイブ ブッシツ ノ ソウ テンイ オヨビ コウアツ ケッショウ カガク ニ カンスル ケンキュウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206234455296","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"不均質なマグマソースから生成された後期中新世∼中期更新世の肥薩火山岩類"},{"@language":"en","@value":"Late Miocene to middle Pleistocene Hisatsu Volcanic Rocks generated from heterogeneous magma sources: Evidence from temporal-spatial variation of distribution and chemistry of the rocks"},{"@value":"不均質なマグマソースから生成された後期中新世～中期更新世の肥薩火山岩類--火山岩の分布と化学組成の時空変化からの証拠"},{"@language":"ja-Kana","@value":"フキンシツ ナ マグマソース カラ セイセイ サレタ コウキ チュウシンセイ チュウキ コウシンセイ ノ ヒサツ カザンガンルイ カザンガン ノ ブンプ ト カガク ソセイ ノ ジクウ ヘンカ カラ ノ ショウコ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679207536512","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Innovation of Thermal Evolution Model of Mantle"},{"@language":"ja","@value":"マントル熱進化モデルの新展開"},{"@language":"ja-Kana","@value":"マントル ネツ シンカ モデル ノ シン テンカイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679207539072","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Have the Japanese Islands Grown?: Five \"Japan\"s Were Born, and Four \"Japan\"s Subducted into the Mantle"},{"@language":"ja","@value":"日本列島の大陸地殻は成長したのか？―５つの日本が生まれ，４つの日本が沈み込み消失した―"},{"@language":"ja-Kana","@value":"ニホン レットウ ノ タイリク チカク ワ セイチョウ シタ ノ カ イツツ ノ ニホン ガ ウマレ ヨッツ ノ ニホン ガ シズミ コミ ショウシツ シタ"},{"@value":"Have the Japanese islands grown?: five “Japan”s were born, and four “Japan”s were subducted into the mantle"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681502662784","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"High-pressure minerals in the Earth and planetary materials"},{"@language":"ja","@value":"地球惑星物質中の高圧鉱物"},{"@language":"ja-Kana","@value":"チキュウ ワクセイ ブッシツ チュウ ノ コウアツ 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