Numerical modeling of trace element transportation in subduction zones : implications for geofluid processes

• 資料種別: 記事
• タイトル: Numerical modeling of trace element transportation in subduction zones : implications for geofluid processes
• 著者・編者: Akihiko Ikemoto; Hikaru Iwamori
• 出版事項: 日本 : Springer science+business media
• 出版年月日等: 2014-04-30
• 出版年（W3CDTF）: 2014-04-30
• タイトル（掲載誌）: EPS : Earth, Planets and Space
• 巻号年月日等（掲載誌）: 66(26)
• 掲載巻: 66(26)
• ISSN（掲載誌）: 1880-5981
• ISSN-L（掲載誌）: 1343-8832
• 本文の言語コード: eng
• DOI: 10.1186/1880-5981-66-26; https://doi.org/10.1186/1880-5981-66-26
• 国立国会図書館永続的識別子: info:ndljp/pid/9227781; https://dl.ndl.go.jp/pid/9227781
• コレクション（共通）: 障害者向け資料
• コレクション（障害者向け資料：レベル1）: テキストデータ
• コレクション（個別）: 国立国会図書館デジタルコレクション > 電子書籍・電子雑誌 > その他; https://dl.ndl.go.jp/collections/B00035
• 収集根拠: オンライン資料収集制度
• 受理日（W3CDTF）: 2015-04-17T10:30:12+09:00
• 保存日（W3CDTF）: 2014-10-10
• 記録形式（IMT）: application/pdf
• オンライン閲覧公開範囲: 国立国会図書館内限定公開
• デジタル化資料送信: 図書館・個人送信対象外
• 遠隔複写可否（NDL）: 可
• 掲載誌（URI）: https://www.earth-planets-space.com/content/66/April/2014
• 掲載誌（国立国会図書館永続的識別子）: info:ndljp/pid/9227755; https://dl.ndl.go.jp/pid/9227755
• 連携機関・データベース: 国立国会図書館 : 国立国会図書館デジタルコレクション; https://dl.ndl.go.jp

• コレクション（個別）: 国立国会図書館デジタルコレクション > デジタル化資料 > 雑誌; https://dl.ndl.go.jp/collections/A00002
• オンライン閲覧公開範囲: 国立国会図書館内限定公開
• デジタル化資料送信: 図書館・個人送信対象外
• 遠隔複写可否（NDL）: 可
• 所蔵機関: 国立国会図書館
• 請求記号: Z19-292
• 掲載誌（国立国会図書館永続的識別子）: info:ndljp/pid/3427594; https://dl.ndl.go.jp/pid/3427594
• 連携機関・データベース: 国立国会図書館 : 国立国会図書館雑誌記事索引; https://ndlsearch.ndl.go.jp
• 書誌ID（NDLBibID）: 9227781; http://id.ndl.go.jp/bib/9227781
• 整理区分コード: 632

• 要約等: コレクション : 国立国会図書館デジタルコレクション > 電子書籍・電子雑誌 > その他
• DOI: 10.1186/1880-5981-66-26; https://doi.org/10.1186/1880-5981-66-26
• オンライン閲覧公開範囲: インターネット公開
• 関連情報（URI）: http://id.ndl.go.jp/digimeta/9227781; https://dl.ndl.go.jp/pid/9227781
• 参照: Enhanced and Asymmetric Melting Beneath the Southern Mariana Back‐Arc Spreading Center Under the Influence of Pacific Plate Subduction; https://cir.nii.ac.jp/crid/1050294485109616640; Special issue ‘Geofluid processes in subduction zones and mantle dynamics’; https://cir.nii.ac.jp/crid/1050845760762911616; Deep slab dehydration and large‐scale upwelling flow in the upper mantle beneath the Japan Sea; https://cir.nii.ac.jp/crid/1360285704779361280; Geochemical mapping of slab-derived fluid and source mantle along Japan arcs; https://cir.nii.ac.jp/crid/1360285707150643200; 地殻流体の起源・分布と変動現象; https://cir.nii.ac.jp/crid/1390001277392720384; Arima hot spring waters as a deep-seated brine from subducting slab; https://cir.nii.ac.jp/crid/2051433317070229760
• 参照: Metastable olivine wedge and deep dry cold slab beneath southwest Japan; https://cir.nii.ac.jp/crid/1360004232135200384; Four‐dimensional numerical modeling of crustal growth at active continental margins; https://cir.nii.ac.jp/crid/1360011143803030912; The Generation and Compaction of Partially Molten Rock; https://cir.nii.ac.jp/crid/1360011143890043776; The chemical composition of subducting sediment and its consequences for the crust and mantle; https://cir.nii.ac.jp/crid/1360011145421838720; A model for disequilibrium mantle melting incorporating melt transport by porous and channel flows; https://cir.nii.ac.jp/crid/1360011145939900928; Trace element transport during dehydration processes in the subducted oceanic crust: 1. Experiments and implications for the origin of ocean island basalts; https://cir.nii.ac.jp/crid/1360011146422800640; Melting and seismic structure beneath the Northeast Japan Arc; https://cir.nii.ac.jp/crid/1360292618713778944; The global range of subduction zone thermal models; https://cir.nii.ac.jp/crid/1360574095468024576; Quantitative analysis of the inclined low-velocity zone in the mantle wedge of northeastern Japan: A systematic change of melt-filled pore shapes with depth and its implications for melt migration; https://cir.nii.ac.jp/crid/1360574095715459584; Speculations on the Consequences and Causes of Plate Motions; https://cir.nii.ac.jp/crid/1360574096089851520; Numerical simulations of subduction zones; https://cir.nii.ac.jp/crid/1360574096138679552; An analysis of the variation of ocean floor bathymetry and heat flow with age; https://cir.nii.ac.jp/crid/1360855567860209920; Simple 2-D models for melt extraction at mid-ocean ridges and island arcs; https://cir.nii.ac.jp/crid/1360855567866151424; Trace element fractionation in deep subduction zones inferred from a lawsonite-eclogite xenolith from the Colorado Plateau; https://cir.nii.ac.jp/crid/1360855568693653632; Petrologic model of the crust and upper mantle of the Japanese Island arcs; https://cir.nii.ac.jp/crid/1360855569066082304; Magma solitons; https://cir.nii.ac.jp/crid/1360855571059812864; Experimentally-determined trace element characteristics of aqueous fluid from partially dehydrated mafic oceanic crust at 3.0 GPa, 650-700C; https://cir.nii.ac.jp/crid/1360855571121084928; Seismological evidence for metastable olivine inside a subducting slab; https://cir.nii.ac.jp/crid/1361137045286285568; Major and trace element composition of the depleted MORB mantle (DMM); https://cir.nii.ac.jp/crid/1361137045590557952; Transportation of H2O and melting in subduction zones; https://cir.nii.ac.jp/crid/1361137045826553344; Boron isotope geochemistry of the oceanic crust from DSDP/ODP Hole 504B; https://cir.nii.ac.jp/crid/1361418518432494080; Contributions of Slab Fluid, Mantle Wedge and Crust to the Origin of Quaternary Lavas in the NE Japan Arc; https://cir.nii.ac.jp/crid/1361418519101857280; Partial Melt Distributions from Inversion of Rare Earth Element Concentrations; https://cir.nii.ac.jp/crid/1361418519498249344; Trace element signature of subduction-zone fluids, melts and supercritical liquids at 120–180 km depth; https://cir.nii.ac.jp/crid/1361418520001753856; The Partitioning of Water Between Nominally Anhydrous Minerals and Silicate Melts; https://cir.nii.ac.jp/crid/1361418521306855936; Water flow to the mantle transition zone inferred from a receiver function image of the Pacific slab; https://cir.nii.ac.jp/crid/1361981470014483968; Zoisite-aqueous fluid trace element partitioning with implications for subduction zone fluid composition; https://cir.nii.ac.jp/crid/1363107368858522880; Experimental melting studies on a model upper mantle composition at high pressure under water-saturated and water-undersaturated conditions; https://cir.nii.ac.jp/crid/1363107369234936448; Serpentine and the subduction zone water cycle; https://cir.nii.ac.jp/crid/1363388846147635328; Emergence of a low-viscosity channel in subduction zones through the coupling of mantle flow and thermodynamics; https://cir.nii.ac.jp/crid/1363951794389558144; SIMS determination of trace element partition coefficients between garnet, clinopyroxene and hydrous basaltic liquids at 2–7.5 GPa and 1080–1200°C; https://cir.nii.ac.jp/crid/1363951794593959808; Partitioning of elements between peridotite and H2O at 2.0–3.0 GPa and 900–1100°C, and application to models of subduction zone processes; https://cir.nii.ac.jp/crid/1363951794951033856; Transportation of H₂O beneath the Japan arcs and its implications for global water circulation; https://cir.nii.ac.jp/crid/1571135651466844544; Geochemical evidence for enhanced fluid flux due to overlapping subducting plates; https://cir.nii.ac.jp/crid/1572824501316275200
• 連携機関・データベース: 国立情報学研究所 : CiNii Research; https://cir.nii.ac.jp/
• 提供元機関・データベース: 雑誌記事索引データベース; https://ndlsearch.ndl.go.jp; Crossref; https://www.crossref.org; 科学研究費助成事業データベース; https://kaken.nii.ac.jp/ja
• 書誌ID（NDLBibID）: 9227781; http://id.ndl.go.jp/bib/9227781