On the evolution of the water ocean in the plate-mantle system
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DOI[10.1186/s40645-018-0209-2]のデータに遷移します
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書誌情報
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- 資料種別
- 記事
- 著者・編者
- Takashi NakagawaHikaru IwamoriRyunosuke Yanagi
- 出版年月日等
- 2018-09-14
- 出版年（W3CDTF）
- 2018-09-14
- タイトル（掲載誌）
- Progress in earth and planetary science
- 巻号年月日等（掲載誌）
- 5(51)
- 掲載巻
- 5(51)
- ISSN（掲載誌）
- 2197-4284
- ISSN-L（掲載誌）
- 2197-4284
- 本文の言語コード
- eng
- DOI
- 10.1186/s40645-018-0209-2
- 国立国会図書館永続的識別子
- info:ndljp/pid/11190346
- コレクション（共通）
- コレクション（障害者向け資料：レベル1）
- 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
- 収集根拠
- オンライン資料収集制度
- 受理日（W3CDTF）
- 2018-11-26T20:20:20+09:00
- 保存日（W3CDTF）
- 2018-11-26
- 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（国立国会図書館永続的識別子）
- info:ndljp/pid/11018906
- 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
- 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）
- 連携機関・データベース
- 国立情報学研究所 : CiNii Research
- 提供元機関・データベース
- 学術機関リポジトリデータベース雑誌記事索引データベースCiNii Articles
- 書誌ID（NDLBibID）
- 11190346
- NII論文ID
- 120006467490
- 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/s40645-018-0209-2
- オンライン閲覧公開範囲
- インターネット公開
- 関連情報
- On the evolution of the water ocean in the plate-mantle system
- 関連情報（URI）
- 参照
- Hydration and Dehydration in Earth's InteriorOn the implications of the coupled evolution of the deep planetary interior and the presence of surface ocean water in hydrous mantle convectionLarge-scale structures in the Earth’s interior: Top-down hemispherical dynamics constrained by geochemical and geophysical approachesDynamics in the Uppermost Lower Mantle: Insights into the Deep Mantle Water Cycle Based on the Numerical Modeling of Subducted Slabs and Global-Scale Mantle DynamicsAb Initio Study on the Lower Mantle Minerals地殻流体の起源・分布と変動現象第一原理計算による超高圧地球科学の新展開
- 参照
- The naked planet Earth: Most essential pre-requisite for the origin and evolution of lifeThe pyrite-type high-pressure form of FeOOHSegregation of subducted oceanic crust in the convecting mantleHydrous minerals and the storage of water in the deep mantleGlobal seismic data reveal little water in the mantle transition zoneEffects of water transportation on subduction dynamics: Roles of viscosity and density reductionEmergence of two types of terrestrial planet on solidification of magma oceanStability of hydrous silicate at high pressures and water transport to the deep lower mantleLong‐Term Stability of Plate‐Like Behavior Caused by Hydrous Mantle Convection and Water Absorption in the Deep MantleRoles of Hydrous Lithospheric Mantle in Deep Water Transportation and Subduction DynamicsHydrous mantle transition zone indicated by ringwoodite included within diamondA planet in transition: The onset of plate tectonics on Earth between 3 and 2 Ga?Hydrogen partitioning between melt, clinopyroxene, and garnet at 3 GPa in a hydrous MORB with 6 wt.% H2OLow heat flow inferred from >4 Gyr zircons suggests Hadean plate boundary interactionsNumerical simulations of subduction zonesGlobal-scale water circulation in the Earth's mantle: Implications for the mantle water budget in the early EarthStability of hydrous phase H MgSiO<sub>4</sub>H<sub>2</sub> under lower mantle conditionsOn the numerical modeling of the deep mantle water cycle in global-scale mantle dynamics: The effects of the water solubility limit of lower mantle mineralsInfluence of water on plastic deformation of olivine aggregates: 1. Diffusion creep regimeGlobal electromagnetic induction constraints on transition-zone water content variationsEvolution of U‐Pb and Sm‐Nd systems in numerical models of mantle convection and plate tectonicsOxygen-isotope evidence from ancient zircons for liquid water at the Earth's surface 4,300 Myr agoHadean age for a post-magma-ocean zircon confirmed by atom-probe tomographyDry (Mg,Fe)SiO<sub>3</sub> perovskite in the Earth's lower mantleSr and Nd isotope geochemistry of oceanic basalts and mantle evolutionThermal evolution with a hydrating mantle and the initiation of plate tectonics in the early EarthOn the relative influence of heat and water transport on planetary dynamicsSome mineral physics constraints on the rheology and geothermal structure of Earth’s lower mantleEffects of strongly variable viscosity on three‐dimensional compressible convection in planetary mantlesContinental crust formation on early Earth controlled by intrusive magmatismGlobal water cycle and Earth's thermal evolutionLithospheric deformation induced by loading of the Hawaiian Islands and its implications for mantle rheologyStagnant slab, wet plumes and Cenozoic volcanism in East AsiaSlab dehydration in the Earth's mantle transition zoneModelling compressible mantle convection with large viscosity contrasts in a three-dimensional spherical shell using the yin-yang gridEfficient cooling of rocky planets by intrusive magmatismShear deformation of bridgmanite and magnesiowüstite aggregates at lower mantle conditionsVolatile accretion history of the terrestrial planets and dynamic implicationsRheology of the Upper Mantle: A SynthesisMelting-induced crustal production helps plate tectonics on Earth-like planetsSubduction factory: 4. Depth-dependent flux of H<sub>2</sub>O from subducting slabs worldwideWater transportation from the subducting slab into the mantle transition zoneEffects of low-viscosity post-perovskite on thermo-chemical mantle convection in a 3-D spherical shellIs the transition zone an empty water reservoir? Inferences from numerical model of mantle dynamicsRecognizable primary volcanic and sedimentary features in a low‐strain domain of the highly deformed, oldest known (≈ 3.7–3.8 Gyr) Greenstone Belt, Isua, West GreenlandWhy is terrestrial subduction one-sided?Modeling mantle convection in the spherical annulusFluid flow in subduction zones: The role of solid rheology and compaction pressureA new analysis of experimental data on olivine rheologyInternally consistent thermodynamic data set for dense hydrous magnesium silicates up to 35GPa, 1600°C: Implications for water circulation in the Earth's deep mantleThe stability of hydrous silicates in Earth's lower mantle: Experimental constraints from the systems MgO–SiO2–H2O and MgO–Al2O3–SiO2–H2OParameters controlling dynamically self‐consistent plate tectonics and single‐sided subduction in global models of mantle convectionSerpentine and the subduction zone water cycleWATER, MELTING, AND THE DEEP EARTH H<sub>2</sub>O CYCLEMantle convection with a brittle lithosphere: thoughts on the global tectonic styles of the Earth and VenusThe origins and concentrations of water, carbon, nitrogen and noble gases on EarthThe effects of deep water cycling on planetary thermal evolutionWater distribution across the mantle transition zone and its implications for global material circulationStability of a hydrous δ-phase, AlOOH–MgSiO<sub>2</sub>(OH)<sub>2</sub>, and a mechanism for water transport into the base of lower mantle38-37億年前のグリーンランド・イスア表成岩帯にみられる世界最古の枕状溶岩Origin of Earth’s oceans: An assessment of the total amount, history and supply of waterTransportation of H<sub>2</sub>O beneath the Japan arcs and its implications for global water circulation
- 参照（URI）
- 連携機関・データベース
- 国立情報学研究所 : CiNii Research
- 提供元機関・データベース
- 雑誌記事索引データベースCrossref科学研究費助成事業データベース科学研究費助成事業データベース科学研究費助成事業データベース科学研究費助成事業データベース科学研究費助成事業データベース学術機関リポジトリデータベースCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossref
- 書誌ID（NDLBibID）
- 11190346