The chemical case for Mercury mantle stripping
国立国会図書館館内限定公開
収録元データベースで確認する
国立国会図書館デジタルコレクション
デジタルデータあり
公開元のウェブサイトで確認する
DOI[10.1186/s40645-019-0312-z]のデータに遷移します
全国の図書館の所蔵
国立国会図書館以外の全国の図書館の所蔵状況を表示します。
所蔵のある図書館から取寄せることが可能かなど、資料の利用方法は、ご自身が利用されるお近くの図書館へご相談ください
書誌情報
この資料の詳細や典拠(同じ主題の資料を指すキーワード、著者名)等を確認できます。
- 資料種別
- 記事
- 著者・編者
- George HelffrichRamon BrasserAnat Shahar
- 出版年月日等
- 2019-12-11
- 出版年(W3CDTF)
- 2019-12-11
- タイトル(掲載誌)
- Progress in earth and planetary science
- 巻号年月日等(掲載誌)
- 6(66)
- 掲載巻
- 6(66)
- 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/s40645-019-0312-z
- 国立国会図書館永続的識別子
- info:ndljp/pid/11467722
- 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)
- 2020-03-23T18:58:42+09:00
- 保存日(W3CDTF)
- 2020-03-23
- 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/11249488
- 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
- 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/s40645-019-0312-z
- 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)
- 参照
- Thermal evolution of Earth and Moon growing by planetesimal impactsSurvey and evaluation of eucrite bulk compositionsThe Elusive Origin of MercuryCrystallization of silicon dioxide and compositional evolution of the Earth’s coreThe origin of eucrites, diogenites, and olivine diogenites: Magma ocean crystallization and shallow magma chamber processes on VestaIs Vesta an intact and pristine protoplanet?The redox state, FeO content, and origin of sulfur‐rich magmas on MercuryThe Major-Element Composition of Mercury’s Surface from MESSENGER X-ray SpectrometrySilicon isotopes in meteorites and planetary core formationThe Chemical Composition of MercuryAccretion of the Earth and segregation of its coreGeochemistry of mantle–core differentiation at high pressureMercury’s inner core size and core-crystallization regimeCollisional stripping of Mercury's mantleThe Origin of MercuryA finite strain approach to thermal expansivity’s pressure dependenceAccretion and differentiation of the terrestrial planets with implications for the compositions of early-formed Solar System bodies and accretion of waterSilicon Isotope Evidence Against an Enstatite Chondrite EarthCarbon in the coreMelting of Peridotite to 140 GigapascalsPressure–temperature cartography of Fe–S–Si immiscible systemVariations in the abundance of iron on Mercury’s surface from MESSENGER X-Ray Spectrometer observationsThermodynamic description for concentrated metallic solutions using interaction parametersThe composition of the EarthThe chemical composition of the Earth: Enstatite chondrite modelsThe interior structure of Mercury constrained by the low-degree gravity field and the rotation of MercuryMercury and other iron-rich planetary bodies as relics of inefficient accretionThe interior structure of Mercury and its core sulfur contentComparative geochemistry of basalts from the moon, earth, HED asteroid, and Mars: implications for the origin of the moonHigh pressure metal–silicate partitioning of Ni, Co, V, Cr, Si, and OTidal constraints on the interior of VenusChondritic models of 4 Vesta: Implications for geochemical and geophysical propertiesMercurian impact ejecta: Meteorites and mantleThe curious case of Mercury's internal structureHigh-temperature Si isotope fractionation between iron metal and silicateExperimental determination of the Si isotope fractionation factor between liquid metal and liquid silicateThe origin of boninites on Mercury: An experimental study of the northern volcanic plains lavasDawn at Vesta: Testing the Protoplanetary ParadigmMetal–silicate partitioning of Mo and W at high pressures and temperatures: Evidence for late accretion of sulphur to the EarthHeterogeneous accretion, composition and core–mantle differentiation of the EarthCore formation and the oxidation state of the EarthMetal–silicate partitioning of sulphur, new experimental and thermodynamic constraints on planetary accretionMetal–silicate silicon isotope fractionation in enstatite meteorites and constraints on Earth's core formationGeodesy constraints on the interior structure and composition of MarsAn Oxygen Isotope Mixing Model for the Accretion and Composition of Rocky PlanetsPartitioning of oxygen between the Earth's mantle and coreSulfur solubility in reduced mafic silicate melts: Implications for the speciation and distribution of sulfur on MercurySilicon in the Earth’s coreThe Role of Reducing Conditions in Building MercurySignificant depletion of volatile elements in the mantle of asteroid Vesta due to core formationExperimental constraints on Mercury's core compositionConstraints on the abundance of carbon in near-surface materials on Mercury: Results from the MESSENGER Gamma-Ray SpectrometerVenusThe effect of Si on metal–silicate partitioning of siderophile elements and implications for the conditions of core formationThermodynamic Modeling of Fe–C–S Ternary System
- 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
- 書誌ID(NDLBibID)
- 11467722