Melting phase relations in the MgSiO3–CaSiO3 system at 24 Gpa
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- Material Type
- 記事
- Author/Editor
- Ryuichi NomuraYoumo ZhouTetsuo Irifune
- Publication, Distribution, etc.
- Publication Date
- 2017-11-28
- Publication Date (W3CDTF)
- 2017-11-28
- Periodical title
- Progress in earth and planetary science
- No. or year of volume/issue
- 4(34)
- Volume
- 4(34)
- ISSN (Periodical Title)
- 2197-4284
- ISSN-L (Periodical Title)
- 2197-4284
- Text Language Code
- eng
- DOI
- 10.1186/s40645-017-0149-2
- Persistent ID (NDL)
- info:ndljp/pid/11018897
- 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)
- 2018-01-12T20:31:06+09:00
- Date Captured (W3CDTF)
- 2018-01-10
- 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/s40645-017-0149-2
- Access Restrictions
- インターネット公開
- Related Material (URI)
- Is Referenced By
- Hadean mantle oxidation inferred from melting of peridotite under lower-mantle conditionsPartitioning of Fe2+ and Fe3+ between bridgmanite and silicate melt: Implications for redox evolution of the Earth's mantlePartial melt composition of enstatite chondritic mantle around the rheological transition at 23 GPa: Implications for the chemical differentiation of the Earth's mantle
- References
- First-principles simulations of CaO and CaSiO3 liquids: structure, thermodynamics and diffusionMeasurement of melting temperatures of some minerals under lower mantle pressuresMelting Curve of MgO from First-Principles SimulationsMelting temperatures of MgO under high pressure by micro-texture analysisStability region of K0.2Na0.8AlSi3O8 hollandite at 22 GPa and 2273 KMelting relations in the MgO–MgSiO3 system up to 70 GPaAbsence of an aluminous phase in the upper part of the Earth's lower mantleSelf-consistent thermodynamic description of silicate liquids, with application to shock melting of MgO periclase and MgSiO<sub>3</sub>perovskitePhase Diagrams for GeoscientistsMelting experiments on the enstatite-diopside join at 70-224 kbar, including the melting of diopsideSolid solution behaviour of CaSiO3 and MgSiO3 perovskitesMelting behavior of (Mg,Fe)O solid solutions at high pressureThermodynamics of mantle minerals - II. Phase equilibriaThe melting curve of perovskite under lower mantle pressuresPhase transition in CaSiO3 perovskiteExperimental constraints on melting temperatures in the MgO–SiO2 system at lower mantle pressuresMelting experiments of mantle materials under lower mantle conditions with implications for magma ocean differentiationMelting phase relations in the MgO–MgSiO3 system between 16 and 26GPa: Implications for melting in Earth's deep interiorHigh‐pressure melting of MgO from (Mg,Fe)O solid solutionsSeismic Evidence for Partial Melt at the Base of Earth's MantleHigh‐pressure phase transformation in CaMgSi<sub>2</sub>O<sub>6</sub> and implications for origin of ultra‐deep diamond inclusionsThermodynamics of mantle minerals - I. Physical propertiesMelting of (Mg, Fe)SiO <sub>3</sub> -Perovskite to 625 Kilobars: Indication of a High Melting Temperature in the Lower MantleMelting of CaSiO<sub>3</sub> perovskite to 430 kbar and first <i>in‐situ</i> measurements of lower mantle eutectic temperaturesExperimentally determined postspinel transformation boundary in Mg<sub>2</sub>SiO<sub>4</sub> using MgO as an internal pressure standard and its geophysical implicationsIn situ determination of the phase boundary between Wadsleyite and Ringwoodite in Mg<sub>2</sub>SiO<sub>4</sub>Constraints on the melting temperature of the lower mantle from high-pressure experiments on MgO and magnesioüstiteThe Phase Boundary Between α- and β-Mg <sub>2</sub> SiO <sub>4</sub> Determined by in Situ X-ray ObservationThe fate of subducted basaltic crust in the Earth's lower mantleModeling the melting of multicomponent systems: the case of MgSiO3 perovskite under lower mantle conditionsMelting and subsolidus relations of SiO<sub>2</sub> at 9–14 GPa
- Data Provider (Database)
- 国立情報学研究所 : CiNii Research
- Original Data Provider (Database)
- 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科学研究費助成事業データベースCrossrefCrossrefCrossref
- Bibliographic ID (NDL)
- 11018897