Element partitioning constraints on the light element composition of the Earth's core

Geophysical Research Letters

Volumn 28, Issue 1, 2001, Pages 81-84

  Li, J ^a   Agee, C B ^a  

^a GEOPHYSICAL LABORATORY   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

EARTH (PLANET); IRON ALLOYS; OXYGEN; PRESSURE EFFECTS; SILICATES; SILICON; SULFUR; THERMAL EFFECTS;

ELEMENT PARTITIONING CONSTRAINTS;

GEOPHYSICS;

CORE (PLANETARY); EXPERIMENTAL MINERALOGY; OXYGEN; PARTITIONING; SILICON; SULFUR;

EID: 0034745211     PISSN: 00948276     EISSN: None     Source Type: Journal    
DOI: 10.1029/2000GL012114     Document Type: Article

References (22)

1. P-T phase diagram for the Allende meteorite
2. High-pressure experiments and the phase diagram of lower mantle and core materials
3. Density and composition of mantle and core
4. Accretion and primary differentiation of the Earth: A personal journey
5. Cosmochemical constraints on the sulfur content in the Earth's core
6. The effect of temperature on the partitioning of nickel, cobalt, manganese, chromium, and vanadium at 9 GPa and constraints on formation of the Earth's core
7. Evidence for a late chondritic veneer in the Earth's mantle from high-pressure partitioning of palladium and platinum
8. Reactions between molten iron and silicate melts at high pressure: Implications for the chemical evolution of Earth's core
9. Chemical analyses of meteorites: A compilation of stony and iron meteorite analyses
10. Metal-silicate partitioning and the incompatibility of S and Si during core formation
11. Geochemistry of mantle-core differentiation at high pressure
12. The composition of the Earth
13. Composition of the core, I: Solubility of oxygen in molten iron at high temperatures
14. Composition of the core, II. Effect of high pressure on solubility of FeO in molten iron
15. Oxide-Metal equilibria to 2500 C and 25 GPa: Implications for core formation and the light component in the Earth's core
16. Light elements in the Earth's outer core: A critical review
17. Prediction of siderophile element metal-silicate partition coefficients to 20 GPa and 2800C: The effects of pressure, temperature, oxygen fugacity, and silicate and metallic melt compositions
18. Models of the Earth's core
19. The influence of pressure and temperature on the metal-silicate partition coefficients of nickel and cobalt in a model C1 chondrite and implications for metal segregation in a deep magma ocean
20. Partitioning "equilibrium" Temperature gradients, and constraints on Earth differentiation
21. Superheating effects on metal-silicate partitioning of siderophile elements
22. Sulfide saturation of basalt and andesite melts at high pressures and temperatures