{"@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/1361137045990174848.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1111/j.1440-1738.1998.00194.x"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1440-1738.1998.00194.x"}},{"identifier":{"@type":"URI","@value":"https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1440-1738.1998.00194.x"}}],"dc:title":[{"@value":"Petrogenesis of the Tanzawa plutonic complex, central Japan: Exposed felsic middle crust of the Izu–Bonin – Mariana arc"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>The Miocene Tanzawa plutonic complex, consisting mainly of tonalite intrusions, is exposed at the northern end of the Izu–Bonin – Mariana (IBM) arc system as a consequence of collision with the Honshu Arc. The Tanzawa plutonic rocks belong to the calc‐alkaline series and exhibit a wide range of chemical variation, from 43 to 75 wt% SiO<jats:sub>2</jats:sub>. They are characterized by relatively high Ba/Rb and Ce/Nb ratios, and low abundances of K<jats:sub>2</jats:sub>O, LIL elements, and rare earth elements (REE). Their petrographic and geochemical features indicate derivation from an intermediate parental magma through crystal fractionation and accumulation processes, involving hornblende, plagioclase, and magnetite. The Tanzawa plutonic complex is interpreted to be the exposed middle crust of the IBM arc, which was uplifted during the collision. The mass balance calculations, combining data from melting experiments of hydrous basaltic compositions at lower‐to‐middle crustal levels, suggest that parental magma and ultramafic restite were generated by dehydration partial melting (∼ 45% melting) of amphibolite chemically similar to low‐K tholeiitic basalt. Partial melting of hydrated mafic lower crust might play an important role in felsic middle‐crust formation in the IBM arc.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1381137045990174848","@type":"Researcher","foaf:name":[{"@value":"SHINICHI KAWATE"}]},{"@id":"https://cir.nii.ac.jp/crid/1381137045990174849","@type":"Researcher","foaf:name":[{"@value":"MAKOTO ARIMA"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"10384871"},{"@type":"EISSN","@value":"14401738"},{"@type":"PISSN","@value":"https://id.crossref.org/issn/10384871"},{"@type":"PISSN","@value":"http://id.crossref.org/issn/10384871"}],"prism:publicationName":[{"@value":"Island Arc"}],"dc:publisher":[{"@value":"Wiley"}],"prism:publicationDate":"1998-07","prism:volume":"7","prism:number":"3","prism:startingPage":"342","prism:endingPage":"358"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1440-1738.1998.00194.x"},{"@id":"https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1440-1738.1998.00194.x"}],"createdAt":"2004-09-29","modifiedAt":"2023-10-28","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050863329678427264","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Influence of stream channel characteristics on bed morphology and step–pool structure in a rhyolitic headstream watershed"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002217652537984","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Missing Oligocene Crust of the Izu-Bonin Arc: Consumed or Rejuvenated During Collision?"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004230839426304","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Intraoceanic Subduction Zone"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004232324651776","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Origin and geodynamic setting of Late Cenozoic granitoids in Sulawesi, Indonesia"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004232456222336","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Late Proterozoic juvenile arc metatonalite and adakitic intrusions in the Sør Rondane Mountains, eastern Dronning Maud Land, Antarctica"}]},{"@id":"https://cir.nii.ac.jp/crid/1360013168780126848","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Structural characteristics of pools in headstream areas"}]},{"@id":"https://cir.nii.ac.jp/crid/1360283691038658176","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Transformation of juvenile Izu–Bonin–Mariana oceanic arc into mature continental crust: An example from the Neogene Izu collision zone granitoid plutons, Central Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360283691683362688","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Structure and growth of the Izu‐Bonin‐Mariana arc crust: 2. 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ケイセイ"},{"@value":"Formation of Continental Crust at the Izu&ndash;Honshu Collision Zone"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206237705984","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Distribution of tonalitic soil structure and geochemistry in the western part of Tanzawa Mountains: Construction of basic data for long-term monitoring study"},{"@language":"ja","@value":"西丹沢中川上流域に分布するトーナル岩母材土壌の構造と地球化学的特性：長期モニタリングに向けた基盤データの構築"},{"@language":"ja-Kana","@value":"ニシタンザワ ナカガワ ジョウリュウイキ ニ ブンプスル トーナルガン ボザイ ドジョウ ノ コウゾウ ト チキュウ カガクテキ トクセイ チョウキ モニタリング ニ ムケタ キバン データ ノ コウチク"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206525928960","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Special Issue “Japanese granites and tectonics” Preface"},{"@language":"ja","@value":"特集号「日本の花崗岩とテクトニクス」緒言"},{"@language":"ja-Kana","@value":"トクシュウゴウ 「 ニホン ノ ハナオカガン ト テクトニクス 」 ショゲン"},{"@value":"Special Issue ^|^ldquo;Japanese granites and tectonics^|^rdquo; Preface"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206525953536","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"K-Ar ages of volcanic rocks in the Tanzawa-Oiso area, central Japan: Implication for westward migration of the Pliocene volcanic front in the southern Fossa Magna region"},{"@language":"ja","@value":"丹沢-大磯地域に分布する火山岩類の K-Ar 年代と南部フォッサマグナ地域における鮮新世火山フロントの西方移動"},{"@language":"ja-Kana","@value":"タンザワ-オオイソ チイキ ニ ブンプ スル カザンガンルイ ノ K-Ar ネンダイ ト ナンブ フォッサマグナ チイキ ニ オケル センシンセイ カザン フロント ノ サイホウ イドウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681213742976","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Genesis and evolutional processes of the Paleozoic oceanic island arc crust, Asago body of the Yakuno Ophiolite, Southwest Japan"},{"@language":"ja","@value":"夜久野オフィオライト朝来岩体における古生代海洋内島弧地殻の形成と進化過程"},{"@value":"夜久野オフィオライト朝来岩体における古生代海洋内島弧地殻の形成と進化"},{"@language":"ja-Kana","@value":"ヤクノ オフィオライト アサゴガンタイ ニ オケル コセイダイ カイヨウナイ トウコ チカク ノ ケイセイ ト シンカ"},{"@value":"Genesis and evolution processes of the Paleozoic oceanic island arc crust, Asago body of the Yakuno ophiolite, Southwest Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681214122496","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Anisotropy of magnetic susceptibility of tonalite in the Tanzawa plutonic complex and its implications for emplacement mechanism."},{"@language":"ja","@value":"帯磁率異方性からみた丹沢トーナル岩体の貫入・定置機構"},{"@language":"ja-Kana","@value":"タイジリツ イホウセイ カラ ミタ タンザワ トーナルガンタイ ノ カンニュウ テイチ キコウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681214301824","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Paleostress history estimated from preferred orientation of microcracks in the Tanzawa tonalite body, central Japan and its relationship to the Honshu arc-Izu arc collision"},{"@language":"ja","@value":"丹沢トーナル岩体における石英中のマイクロクラックから推定された古応力場の変遷と伊豆弧の衝突"},{"@language":"ja-Kana","@value":"タンザワ トーナルガンタイ ニ オケル セキエイ チュウ ノ マイクロクラック カラ スイテイ サレタ コ オウリョクバ ノ ヘンセン ト イズ コ ノ ショウトツ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681218251136","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Geology of the Tanzawa Mountains, Japan:"},{"@language":"ja","@value":"丹沢山地の地質："},{"@value":"丹沢山地の地質 : 伊豆衝突帯のジオダイナミクス"},{"@language":"ja-Kana","@value":"タンザワ サンチ ノ チシツ : イズ ショウトツタイ ノ ジオダイナミクス"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681502775296","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"海洋性島弧から大陸地殻へ：伊豆衝突帯花崗岩質岩体の成因研究"},{"@language":"en","@value":"Transformation of oceanic arc into continental crust: Petrogenetic study on the Izu Collision Zone granitoid plutons"},{"@value":"日本鉱物科学会研究奨励賞第14回受賞者 受賞記念研究紹介 海洋性島弧から大陸地殻へ : 伊豆衝突帯花崗岩質岩体の成因研究"},{"@language":"ja-Kana","@value":"ニホン コウブツ カガクカイ ケンキュウ ショウレイショウ ダイ14カイ ジュショウシャ ジュショウ キネン ケンキュウ ショウカイ カイヨウセイ トウコ カラ タイリク チカク エ : イズ ショウトツタイ ハナオカガンシツガンタイ ノ セイイン ケンキュウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681503069952","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Geochemical diversity of Neogene granitoid plutons in the Izu Collision Zone: implications for transformation of juvenile oceanic arc into mature continental 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