| scholarly article | Q13442814 |
| P6179 | Dimensions Publication ID | 1013041873 |
| P356 | DOI | 10.1038/42685 |
| P2888 | exact match | https://scigraph.springernature.com/pub.10.1038/42685 |
| P50 | author | Catherine McCammon | Q87265457 |
| P2860 | cites work | Absence of an aluminous phase in the upper part of the Earth's lower mantle | Q59081249 |
| X-ray microanalysis of high-pressure/high-temperature phases synthesized from natural olivine in a diamond-anvil cell | Q63947459 | ||
| The mineralogy and chemistry of the lower mantle: an implication of the ultrahigh-pressure phase relations in the system MgOFeOSiO2 | Q107274973 | ||
| Partitioning of MgO, FeO, NiO, MnO and Cr2O3 between magnesian silicate perovskite and magnesiowüstite: implications for the origin of inclusions in diamond and the composition of the lower mantle | Q107275011 | ||
| Experimental determination of element partitioning and calculation of phase relations in the MgO-FeO-SiO2 system at high pressure and high temperature | Q107275407 | ||
| DAC measurement of perovskite conductivity and implications for the distribution of mineral phases in the lower mantle | Q107275418 | ||
| The Effect of Alumina on Phase Transformations at the 660-Kilometer Discontinuity from Fe-Mg Partitioning Experiments | Q107275654 | ||
| P433 | issue | 6634 | |
| P407 | language of work or name | English | Q1860 |
| P921 | main subject | perovskite | Q409787 |
| perovskite structure | Q3036449 | ||
| P304 | page(s) | 694-696 | |
| P577 | publication date | 1997-06-01 | |
| P1433 | published in | Nature | Q180445 |
| P1476 | title | Perovskite as a possible sink for ferric iron in the lower mantle | |
| P478 | volume | 387 |
| Q107271024 | A mineralogical model for density and elasticity of the Earth's mantle |
| Q44564728 | Accretion and core formation: constraints from metal-silicate partitioning |
| Q56442885 | Accretion of the Earth and segregation of its core |
| Q60912000 | Altered chemistry of oxygen and iron under deep Earth conditions |
| Q58983138 | Aluminium under the spotlight |
| Q107269637 | Cationic substitution in MgSiO3 perovskite |
| Q30999000 | Chemical interaction of Fe and Al(2)O3 as a source of heterogeneity at the Earth's core-mantle boundary |
| Q60432788 | Compressibility of brownmillerite (Ca2Fe2O5): effect of vacancies on the elastic properties of perovskites |
| Q64387126 | Computational support for a pyrolitic lower mantle containing ferric iron |
| Q60432764 | Crystal structure and equation of state of MgSiO3perovskite |
| Q60369165 | Effect of iron oxidation state on the electrical conductivity of the Earth’s lower mantle |
| Q107271111 | Elastic anisotropy of FeSiO3 end-members of the perovskite and post-perovskite phases |
| Q59066714 | Electrical conductivity of silicate perovskite at lower-mantle conditions |
| Q33417206 | Electronic and magnetic structures of the postperovskite-type Fe2O3 and implications for planetary magnetic records and deep interiors |
| Q37557390 | Electronic spin state of iron in lower mantle perovskite |
| Q107271114 | Electronic spin transitions and the seismic properties of ferrous iron-bearing MgSiO3 post-perovskite |
| Q63947358 | Equation of state of Al-bearing perovskite to lower mantle pressure conditions |
| Q107275374 | Evaluation of (Mg,Fe) partitioning between silicate perovskite and magnesiowustite up to 120 GPa and 2300 K |
| Q36306904 | Evidence for a Fe3+-rich pyrolitic lower mantle from (Al,Fe)-bearing bridgmanite elasticity data |
| Q107271110 | Fe3+and Al solubilities in MgSiO3 perovskite: implication of the Fe3+AlO3 substitution in MgSiO3 perovskite at the lower mantle condition |
| Q59841271 | Ferric iron in Al-bearing post-perovskite |
| Q107275357 | Garnet-perovskite transformation under conditions of the Earth's lower mantle: an analytical transmission electron microscopy study |
| Q64055111 | Hydrous magnesium-rich magma genesis at the top of the lower mantle |
| Q105605131 | Influence of Hydrogen-Related Defects on the Electrical Conductivity and Plastic Deformation of Mantle Minerals: A Critical Review |
| Q60722222 | Influence of Water on Major Phase Transitions in the Earth's Mantle |
| Q58809959 | Iron speciation in minerals and glasses probed by $$\hbox{M}_{2/3}$$ M 2 / 3 -edge X-ray Raman scattering spectroscopy |
| Q57235557 | Long-term fluxes and budget of ferric iron: implication for the redox states of the Earth's mantle and atmosphere |
| Q105603069 | Mantle oxidation state and oxygen fugacity: Constraints on mantle chemistry, structure, and dynamics |
| Q107275321 | Melting relations and major element partitioning in an oxidized bulk Earth model composition at 15–26 GPa |
| Q57866728 | Optical signatures of low spin Fe3+ in NAL at high pressure |
| Q107275437 | Oxide-metal equilibria to 2500°C and 25 GPa: Implications for core formation and the light component in the Earth's core |
| Q105603077 | Oxygen Vacancy Substitution Linked to Ferric Iron in Bridgmanite at 27 GPa |
| Q107269630 | Partitioning of iron between magnesian silicate perovskite and magnesiowüstite at about 1 Mbar |
| Q105594530 | Peridotite melting and mineral–melt partitioning of major and minor elements at 22–24.5 GPa |
| Q107271093 | Phase relation and mineral chemistry in pyrolite to 2200°C under the lower mantle pressures and implications for dynamics of mantle plumes |
| Q107275311 | Phase transformations and partitioning relations in peridotite under lower mantle conditions |
| Q107288534 | Phase transformations: Implications for mantle structure |
| Q57883343 | Poisson's ratio in the lower mantle beneath Alaska: Evidence for compositional heterogeneity |
| Q60714818 | Prediction of a new phase transition in Al2O3at high pressures |
| Q59056656 | Pressure-induced changes in the compression mechanism of aluminous perovskite in the Earth's mantle |
| Q107275376 | Pressure-volume-temperature equation of state of MgSiO3 perovskite from molecular dynamics and constraints on lower mantle composition |
| Q46284153 | Radiative conductivity in the Earth's lower mantle |
| Q57866579 | Silicon self-diffusion in MgSiO3 perovskite at 25 GPa |
| Q36137879 | Spin and valence dependence of iron partitioning in Earth's deep mantle |
| Q59060854 | Spin crossover and iron-rich silicate melt in the Earth’s deep mantle |
| Q105603082 | Stability and Solubility of the FeAlO 3 Component in Bridgmanite at Uppermost Lower Mantle Conditions |
| Q48325598 | Stability of ferrous-iron-rich bridgmanite under reducing midmantle conditions |
| Q107275371 | Subsolidus and melting experiments of K-doped peridotite KLB-1 to 27 GPa: Its geophysical and geochemical implications |
| Q105594531 | The effect of Al 2 O 3 on Fe–Mg partitioning between magnesiowüstite and magnesium silicate perovskite |
| Q107275370 | The electrical conductivity of the lower mantle phase magnesiowüstite at high temperatures and pressures |
| Q38456740 | The origin of the terrestrial noble-gas signature |
| Q59841113 | The valence state and partitioning of iron in the Earth's lowermost mantle |
| Q63947336 | Thermochemical state of the lower mantle: New insights from mineral physics |
| Q33518413 | Thickness and Clapeyron slope of the post-perovskite boundary. |
| Q57866498 | Water solubility in Mg-perovskites and water storage capacity in the lower mantle |
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