Melting relations in the Fe-S-Si system at high pressure and temperature : implications for the planetary core
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- Material Type
- 記事
- Author/Editor
- Takanori SakairiEiji OhtaniSeiji Kamada
- Publication, Distribution, etc.
- Publication Date
- 2017-03-31
- Publication Date (W3CDTF)
- 2017-03-31
- Periodical title
- Progress in earth and planetary science
- No. or year of volume/issue
- 4(10)
- Volume
- 4(10)
- ISSN (Periodical Title)
- 2197-4284
- ISSN-L (Periodical Title)
- 2197-4284
- Text Language Code
- eng
- DOI
- 10.1186/s40645-017-0125-x
- Persistent ID (NDL)
- info:ndljp/pid/10369587
- Collection
- Collection (Materials For Handicapped People:1)
- Collection (particular)
- 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
- Acquisition Basis
- オンライン資料収集制度
- Date Accepted (W3CDTF)
- 2017-06-29T04:49:44+09:00
- Date Captured (W3CDTF)
- 2017-06-26
- Format (IMT)
- application/pdf
- Access Restrictions
- 国立国会図書館内限定公開
- Service for the Digitized Contents Transmission Service
- 図書館・個人送信対象外
- Availability of remote photoduplication service
- 可
- Periodical Title (URI)
- Periodical Title (Persistent ID (NDL))
- info:ndljp/pid/10369577
- Data Provider (Database)
- 国立国会図書館 : 国立国会図書館デジタルコレクション
- Summary, etc.
- 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/s40645-017-0125-x
- Access Restrictions
- インターネット公開
- Related Material (URI)
- Is Referenced By
- Melting experiments on Fe–Si–S alloys to core pressures: Silicon in the core?Synoptic conditions and potential causes of the extreme heavy rainfall event of January 2009 over Mindanao Island, PhilippinesOn the Melting of Alloys FeX (X = Ni, Ta, Nb, Cr) under Pressure up to 5 GPa
- References
- Density measurements of liquid Fe–Si alloys at high pressure using the sink–float methodThe structure of Fe‐Ni alloy in Earth's inner coreDensity measurement of liquid FeS at high pressures using synchrotron X-ray absorptionNew high-pressure and high-temperature metal/silicate partitioning of U and Pb: Implications for the cores of the Earth and MarsSome aspects of core formation in MercuryDecomposition of Fe<sub>3</sub>S above 250 GPaMelting relationships in the Fe–Fe3S system up to the outer core conditionsHighly intense monochromatic X-ray diffraction facility for high-pressure research at SPring-8Interaction between iron and post‐perovskite at core‐mantle boundary and core signature in plume source regionHighly reducing conditions during core formation on Mercury: Implications for internal structure and the origin of a magnetic fieldDensity profile of an SNC model Martian interior and the moment-of-inertia factor of MarsThe chemical composition of the EarthMercury’s inner core size and core-crystallization regimeDensity and composition of mantle and coreAn Experimental Perspective on the Light Element in Earth’s CoreLiquidus and solidus temperatures of a Fe–O–S alloy up to the pressures of the outer core: Implication for the thermal structure of the Earth's coreBemerkungen zur SchmelzdruckkurveFeFeS eutectic temperatures to 620 kbarPhase relations of Fe‐Si alloy up to core conditions: Implications for the Earth inner coreThe Interior of MarsMelting of Peridotite to 140 GigapascalsPressure–temperature cartography of Fe–S–Si immiscible systemInternal structure of Mercury: Implications of a molten coreIron-Silicon Alloy in Earth's Core?Large Longitude Libration of Mercury Reveals a Molten CoreIn situ determination of Fe–Fe3S phase diagram and liquid structural properties up to 65 GPaPhysical properties of liquid Fe alloys at high pressure and their bearings on the nature of metallic planetary coresThe integral enstatite chondrite model of the EarthMelting of iron–silicon alloy up to the core–mantle boundary pressure: implications to the thermal structure of the Earth’s corePartial melting in the iron–sulfur system at high pressure: A synchrotron X-ray diffraction studyMars: A New Core-Crystallization RegimeLow-altitude magnetic field measurements by MESSENGER reveal Mercury’s ancient crustal fieldHigh-Pressure Iron-Sulfur Compound, Fe <sub>3</sub> S <sub>2</sub> , and Melting Relations in the Fe-FeS SystemInterior Evolution of MercuryDensity measurements of liquid Fe‐S alloys at high‐pressureEutectic melting in the system Fe–S to 44 GPaThe NaCl pressure standardTheory of thermal and elastic properties of the lower mantle and coreGruneisen parameter of ε-iron up to 300 GPa from in-situ X-ray studyMelting of Iron at Earth’s Inner Core Boundary Based on Fast X-ray DiffractionSulfur's impact on core evolution and magnetic field generation on GanymedeThe Grüneisen parameter for iron at outer core conditions and the resulting conductive heat and power in the coreGrüneisen parameters and isothermal equations of statePhase relations in the system Fe-FeSi at 21 GPaPhase relations in the Fe–FeSi system at high pressures and temperaturesPhase relationships of the Fe–FeS system in conditions up to the Earth's outer coreStructure type and bulk modulus of Fe<sub>3</sub>S, a new iron-sulfur compoundSulfur in the Earth’s inner coreToward an internally consistent pressure scaleMelting experiments on anhydrous peridotite KLB‐1 from 5.0 to 22.5 GPaClosure of the Fe–S–Si liquid miscibility gap at high pressureThermal evolutions of the terrestrial planets鉄-シリコン合金の状態方程式Ｘ線回折実験における統合解析支援ソフトウェアの開発Liquidus and solidus temperature of a Fe-O-S alloy up to the pressures of the outer core: Implication for the thermal structure of the Earth’s core
- Data Provider (Database)
- 国立情報学研究所 : CiNii Research
- Original Data Provider (Database)
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