{"@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/1362825895998230912.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/97jb00788"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F97JB00788"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/97JB00788"}},{"identifier":{"@type":"NAID","@value":"80009802443"}}],"dc:title":[{"@value":"Element transport from slab to volcanic front at the Mariana arc"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>We present a comprehensive geochemical data set for the most recent volcanics from the Mariana Islands, which provides new constraints on the timing and nature of fluxes from the subducting slab. The lavas display many features typical of island arc volcanics, with all samples showing large negative niobium anomalies and enrichments in alkaline earth elements and lead (e.g., high Ba/La and Pb/Ce). Importantly, many of these key ratios correlate with a large range in <jats:sup>238</jats:sup>U excesses, (<jats:sup>238</jats:sup>U/<jats:sup>230</jats:sup>Th) = 0.97–1.56. Geochemical features show island to island variations; lavas from Guguan have the largest <jats:sup>238</jats:sup>U‐excesses, Pb/Ce and Ba/La ratios, while Agrigan lavas have small <jats:sup>238</jats:sup>U excesses, the least radiogenic <jats:sup>143</jats:sup>Nd/<jats:sup>144</jats:sup>Nd, and the largest negative cerium and niobium anomalies. These highly systematic variations enable two discrete slab additions to the subarc mantle to be identified. The geochemical features of the Agrigan lavas are most consistent with a dominant subducted sediment contribution. The added sedimentary component is not identical to bulk subducted sediment and notably shows a marked enrichment of Th relative to Nb. This is most readily explained by melt fractionation of the sediment with residual rutile and transfer of sedimentary material as a melt phase. For most of the highly incompatible elements, the sedimentary contribution dominates the total elemental budgets of the lavas. The characteristics best exemplified by the Guguan lavas are attributed to a slab‐derived aqueous fluid phase, and Pb and Sr isotope compositions point toward the subducted, altered oceanic crust as a source of this fluid. Variable addition of the sedimentary component, but near‐constant aqueous fluid flux along arc strike, can create the compositional trends observed in the Mariana lavas. High field strength element ratios (Ta/Nb and Zr/Nb) of the sediment poor Guguan lavas are higher than those of most mid‐oceanic ridge basalts and suggest a highly depleted subarc mantle prior to any slab additions. The <jats:sup>238</jats:sup>U‐<jats:sup>230</jats:sup>Th systematics indicate >350 kyr between sediment and mantle melting but <30 kyr between slab dehydration and eruption of the lavas. This necessitates rapid magma migration rates and suggests that the aqueous fluid itself may trigger major mantle melting.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1382825895998230913","@type":"Researcher","foaf:name":[{"@value":"Tim Elliott"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825895998230912","@type":"Researcher","foaf:name":[{"@value":"Terry Plank"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825895998231040","@type":"Researcher","foaf:name":[{"@value":"Alan Zindler"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825895998230914","@type":"Researcher","foaf:name":[{"@value":"William White"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825895998230915","@type":"Researcher","foaf:name":[{"@value":"Bernard Bourdon"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"01480227"},{"@type":"PISSN","@value":"https://id.crossref.org/issn/01480227"}],"prism:publicationName":[{"@value":"Journal of Geophysical Research: Solid Earth"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"1997-07-10","prism:volume":"102","prism:number":"B7","prism:startingPage":"14991","prism:endingPage":"15019"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F97JB00788"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/97JB00788"}],"createdAt":"2004-02-03","modifiedAt":"2023-09-22","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360002215857471104","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Geochemistry and petrogenesis of the Eocene back arc mafic rocks in the Zagros suture zone, northern Noorabad, western Iran"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004233285486592","@type":"Article","resourceType":"学術雑誌論文(journal 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<SUP>238</SUP>U-<SUP>230</SUP>Th-<SUP>226</SUP>Ra放射非平衡"}]},{"@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/1390001204237163136","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Chemical Composition of Mantle Wedge Fluids"},{"@language":"ja","@value":"マントルウェッジ流体の化学組成"},{"@language":"ja-Kana","@value":"マントルウェッジ リュウタイ ノ カガク ソセイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204305177088","@type":"Article","resourceType":"学術雑誌論文(journal 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arc"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001205742801408","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"ウラン系列短寿命核種の精密分析法の開発とマグマプロセス解明への応用"},{"@language":"en","@value":"Development of precise isotope analyses of U-series nuclides for the study of U-series disequilibria in magma processes"},{"@value":"2004年度日本地球化学会奨励賞受賞記念論文(The Geochemical Society of Japan Award for Young Researchers) ウラン系列短寿命核種の精密分析法の開発とマグマプロセス解明への応用"},{"@language":"ja-Kana","@value":"2004ネンド ニホン チキュウ カガクカイ ショウレイショウ ジュショウ キネン ロンブン The Geochemical Society of Japan Award for Young Researchers ウラン ケイレツ タンジュミョウカクシュ ノ セイミツ ブンセキホウ ノ カイハツ ト マグマプロセス カイメイ エ ノ オウヨウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206234455296","@type":"Article","relationType":["isReferencedBy","isCitedBy"],"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 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