{"@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/1363388845134607232.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/96jb03661"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F96JB03661"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/96JB03661"}},{"identifier":{"@type":"NAID","@value":"80009606387"}}],"dc:title":[{"@value":"Across‐arc variations of isotope and trace element compositions from Quaternary basaltic volcanic rocks in northeastern Japan: Implications for interaction between subducted oceanic slab and mantle wedge"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>Isotopic compositions of Pb, Sr, and Nd and concentrations of trace elements were determined for Quaternary island arc basaltic rocks from northeastern Japan. Sr and Pb isotopic ratios decrease, and Nd isotopic ratios increase from the volcanic front toward the back arc. The isotopic compositions nearest the back arc side are nearly identical to those of mid‐ocean ridge basalt (MORB). The high field strength elements and heavy rare earth elements show homogeneous and MORB‐like characteristics. These observations indicate that the mantle wedge beneath northeastern Japan originally had a MORB‐type mantle composition that was homogeneous across the arc. Pb isotope compositions show a mixing relationship between mantle wedge and oceanic sediments reflecting the introduction of subduction component into the mantle wedge, Across‐arc isotopic variations were caused by interaction between MORB‐type mantle wedge and the subducting slab, and the amount of subduction component correlates with the depth to the slab. The isotopic compositions of subduction component are expressed by bulk mixing of 15 wt % of oceanic sediment and 85 wt % of altered MORB. Inversion analyses of isotopic compositions using two‐component mixing relationships show that the Sr/Nd and Pb/Nd ratios in subduction component decrease with increasing depth to the slab, while the Sr/Pb ratio is nearly constant. These changes can be explained only by a preferential discharge of the elements into the wedge mantle associated with continuous dehydration of the subducting slab. The present study further demonstrates that a very wide range of isotopic and elemental compositions in island arc magmas is a consequence of the interaction between subducting slab and mantle wedge without the involvement of an oceanic island basalts component, and the slab can carry water and supply a subduction component as a fluid to the overlying mantle wedge to depths exceeding 150 km.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1383388845134607232","@type":"Researcher","foaf:name":[{"@value":"Tomoyuki Shibata"}]},{"@id":"https://cir.nii.ac.jp/crid/1383388845134607233","@type":"Researcher","foaf:name":[{"@value":"Eizo Nakamura"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"01480227"},{"@type":"PISSN","@value":"https://id.crossref.org/issn/01480227"},{"@type":"NCID","@value":"AA10819765"}],"prism:publicationName":[{"@value":"Journal of Geophysical Research: Solid Earth"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"1997-04-10","prism:volume":"102","prism:number":"B4","prism:startingPage":"8051","prism:endingPage":"8064"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F96JB03661"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/96JB03661"}],"createdAt":"2004-02-03","modifiedAt":"2023-09-23","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360004232324568064","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Petrology of peridotite xenolith-bearing basaltic to andesitic lavas from the Shiribeshi Seamount, off northwestern Hokkaido, the Sea of Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004234741767808","@type":"Article","resourceType":"学術雑誌論文(journal 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melts"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848661184635648","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Along-arc geochemical variations in Quaternary magmas of northern Kyushu Island, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204230447872","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Genetic Relationship between Quaternary NE Japan Arc Magmas and Miocene Japan Sea Back-arc Basin Basalts"},{"@value":"東北日本弧と大和海盆周辺のマグマの成因関係"},{"@language":"ja-Kana","@value":"トウホク ニホン コ ト ヤマト カイボン シュウヘン ノ マグマ ノ セイイン カンケイ アツイ ユビ ノ ダイナミック モデル"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204551593600","@type":"Article","relationType":["isReferencedBy","isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Geographical distribution of 3He/4He ratios and seismic tomography in Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001205741905280","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"島弧火山の地球化学的研究"},{"@language":"en","@value":"Geochemical studies on island arc volcanoes"},{"@value":"島弧火山の地球化学的研究(1994年度日本地球化学会賞受賞記念論文)"},{"@language":"ja-Kana","@value":"トウコ カザン ノ チキュウ カガクテキ ケンキュウ 1994ネンド ニホン"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206525021696","@type":"Article","relationType":["isReferencedBy","isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Sr, Nd and Pb isotopic compositions of volcanic rocks from the Inaniwadake district, Northeast Japan arc"},{"@language":"ja","@value":"東北日本弧，稲庭岳地域の火山岩のＳｒ，Ｎｄ，Ｐｂ同位体組成"},{"@language":"ja-Kana","@value":"トウホク ニホンコ イナニワダケ チイキ ノ カザンガン ノ Sr Nd Pb ドウイタイ ソセイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206525709568","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"北部フォッサマグナに産する後期新生代火山岩のSr-Nd 同位体組成からみた 2 つのソースマントルの分布"},{"@language":"en","@value":"The distributions of two mantle sources based on the Sr-Nd isotopic compositions of late Cenozoic volcanic rocks from the northern Fossa Magna, central Japan"},{"@language":"ja-Kana","@value":"ホクブ フォッサマグナ ニ サンスル コウキ シンセイダイ カザンガン ノ Sr-Nd ドウイタイ ソセイ カラ ミタ 2ツ ノ ソースマントル ノ ブンプ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206546546688","@type":"Article","relationType":["isReferencedBy","isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Effect of subduction components on production of basalts from Tateshina volcano, central Japan: geochemical calculation of dehydration of subducting oceanic crust and partial melting of overlying sediments, and subsequent fluid-mantle interaction"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679037229952","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy","isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Interaction between seawater and Miocene volcanic rocks recovered by deep drilling in the Niigata oil and gas fields, northeast Japan-Sr and Nd isotopic evidence from oil and gas-bearing volcanic rocks-"},{"@language":"ja","@value":"新潟油・ガス田地域の中新世火山岩と海水の相互作用―石油・天然ガスを胚胎する火山岩のＳｒおよびＮｄ同位体比―"},{"@language":"ja-Kana","@value":"ニイガタ ユ ガスデン チイキ ノ チュウシンセイ カザンガン ト カイスイ ノ ソウゴ サヨウ セキユ テンネン ガス オ ハイタイスル カザンガン ノ Sr オヨビ Nd ドウイタイヒ"},{"@value":"Interaction between seawater and Miocene volcanic rocks recovered by deep drilling in the Niigata oil and gas fields, northeast Japan—Sr and Nd isotopic evidence from oil and gas-bearing volcanic rocks"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679210994816","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"東北本州弧における後期新生代の火成活動史(<特集>島弧の深部構造-地質・地震・地震波トモグラフィによる解析(II))"},{"@language":"en","@value":"Late Cenozoic Magmatism in the northeast Honshu Arc, Japan(<Special issue>Deep Structure under Island Arcs from the Viewpoints of Geology, Seismology and Seismic Tomography (II))"},{"@value":"東北本州弧における後期新生代の火成活動史"},{"@language":"ja-Kana","@value":"トウホクホンシュウ コ ニ オケル コウキ シンセイダイ ノ カセイカツドウシ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681211278464","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Petrology of Oligocene volcanic rocks from the middle part of the Monzen Formation, Oga Peninsula, northeastern Japan."},{"@value":"男鹿半島，漸新統門前層中部の火山岩類の岩石学"},{"@language":"ja-Kana","@value":"オガ ハントウ ゼンシントウモンゼンソウ チュウブ ノ カザンガンルイ ノ ガンセキガク"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681214381440","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"K-Ar ages and petrology of the Takinoue stage volcanic rocks in central Hokkaido, Japan: Geochemistry of volcanic rocks that form a shallow reservoir in the Yufutsu Oil and Gas Field"},{"@language":"ja","@value":"北海道中央部に分布する滝の上期火山岩類の放射年代と岩石学的特徴－勇払油ガス田の浅層貯留層を構成する火山岩の岩石化学的検討－"},{"@language":"ja-Kana","@value":"ホッカイドウ チュウオウブ ニ ブンプ スル タキノウエ キ カザンガンルイ ノ ホウシャ ネンダイ ト ガンセキガクテキ トクチョウ ユウフツユ ガスデン ノ センソウ チョリュウソウ オ コウセイ スル カザンガン ノ ガンセキ カガクテキ ケントウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681217484928","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Geology and petrology of the Pleistocene Oshima-Kojima volcano, Southwestern Hokkaido"},{"@language":"ja","@value":"西南北海道，更新世渡島小島火山の地質と岩石学的特徴"},{"@language":"ja-Kana","@value":"セイナン ホッカイドウ,コウシン ヨワタリトウ コジマ カザン ノ チシツ ト ガンセキガクテキ トクチョウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681486474624","@type":"Article","relationType":["isReferencedBy","isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Constraints on HIMU and EM by Sr and Nd isotopes re-examined"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681502729984","@type":"Article","relationType":["isReferencedBy","isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Petrology of Late Oligocene volcanic rocks from southern part of central Hokkaido, Japan-Implication for incipient volcanism of back-arc rift-"},{"@language":"ja","@value":"中央北海道南部の後期漸新世火山岩の岩石学的検討‐背弧海盆拡大の初期火山活動‐"},{"@value":"中央北海道南部の後期漸新世火山岩の岩石学的検討 : 背弧海盆拡大の初期火山活動"},{"@language":"ja-Kana","@value":"チュウオウ ホッカイドウ ナンブ ノ コウキゼンシン セイ カザンガン ノ ガンセキガクテキ ケントウ : ハイ コカイボン カクダイ ノ ショキ カザン カツドウ"},{"@value":"Petrology of Late Oligocene volcanic rocks from southern part of central Hokkaido, Japan—Implication for incipient volcanism of back-arc rift—"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681522247680","@type":"Article","relationType":["isReferencedBy","isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Sr-Nd-Pb isotopic and major and trace element compositions of the Yufu-Tsurumi volcanic rocks: implications for the magma genesis of the Yufu-Tsurumi volcanoes, northeast Kyushu, Japan"},{"@value":"Sr–Nd–Pb isotopic and major and trace element compositions of the Yufu–Tsurumi volcanic rocks: implications for the mama genesis of the Yufu–Tsurumi volcanoes, Northeast Kyushu, Japan"},{"@value":"Sr–Nd–Pb isotopic and trace element compositions of the Yufu–Tsurumi volcanic rocks: implications for the magma genesis of the Yufu–Tsurumi volcanoes, Northeast Kyushu, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681523413504","@type":"Article","relationType":["isReferencedBy","isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Trace element and Sr-Nd isotopic features of ultramafic xenoliths from Kurose, Southwest Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1390299915004519040","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Molybdenum isotopic compositions in volcanic rocks 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