Melting relations and major element partitioning in an oxidized bulk Earth model composition at 15-26 GPa

Lithos

Volumn 53, Issue 3-4, 2000, Pages 233-245

  Trønnes, Reidar G ^a,b  

^a UNIVERSITY OF ALBERTA   (Canada)

^b UNIVERSITY OF ICELAND   (Iceland)

Author keywords

Bulk Earth model composition; Element partitioning; Magnesiowustite; Melting relations; Perovskite

Indexed keywords

MAGNESIOWUSTITE; MELTING; PARTITIONING; PEROVSKITE;

EID: 0033833710     PISSN: 00244937     EISSN: None     Source Type: Journal    
DOI: 10.1016/S0024-4937(00)00027-X     Document Type: Article

References (33)

1. A new look at differentiation of the Earth from melting experiments on the Allende meteorite
2. High-pressure melting of carbonaceous chondrite
3. Crystal-liquid density inversions in terrestrial and lunar magmas
4. Pressure-temperature phase diagram for the Allende meteorite
5. Mass balance and density constraints on early differentiation of chondritic mantle
6. The chemical composition of the Earth
7. Abundances of the elements: Meteoritic and solar
8. 5.5
9. Experimental studies of trace element partitioning applicable to igneous petrogenesis - Sedona 16 years later
10. In search of a bulk-Earth composition
11. Generation of plume magmas through time: An experimental perspective
12. Melting experiments on anhydrous KLB-1: Compositions of magmas in the upper mantle and transition zone
13. Melting experiments on komatiite analog compositions at 5 GPa
14. Phase equilibrium constraints on the origin of basalts, picrites and komatiites
15. Experimental trace element partitioning, rock physics and phase relations
16. 3 perovskite at 25 GPa by double-stage multianvil system
17. Determination of Fe-Mg partitioning between perovskite and magnesiowustite
18. 3 between magnesian silicate perovskite and magnesiowustite: Implications for the origin of inclusions in diamond and the composition of the lower mantle
19. Perovskite as a possible sink of ferric iron in the lower mantle
20. Ferric iron content of mineral inclusions in diamonds from Sao Luiz: A view into the lower mantle
21. Magnesiowustite/melt and majorite/melt partitioning and the early thermal history of the Earth
22. The bearing of phase equilibria studies in synthetic and natural systems on the origin of basic and ultrabasic rocks
23. Suspension in convective layers and style of differentiation of a terrestrial magma ocean
24. Magma ocean formation due to giant impacts
25. Melting relations and mineral-melt partitioning of an FeO-rich, bulk Earth model composition at 15-27 GPa. Origin of the Earth and Moon
26. Element partitioning between silicate minerals and coexisting melts at pressures of 1-27 GPa, and implications for mantle evolution
27. Melting of garnet peridotite and the origin of komatiite and depleted lithosphere
28. Formation of the Earth
29. Phase transformations and partitioning relations in peridotite under lower mantle conditions
30. The effect of alumina on phase transformations at the 660-kilometer discontinuity from Fe-Mg partitioning experiments
31. Melting experiments on anhydrous peridotite KLB-1 from 5.0 to 22.5 GPa
32. 2 at 9 to 14 GPa