Peridotite melting and mineral–melt partitioning of major and minor elements at 22–24.5 GPa

By R. Trønnes, D. Frost. 2002

152 citations recorded by the source corpus.

Subfields: Geophysics

View Paper: https://www.semanticscholar.org/paper/975c1b254f0f85eb7ef70b263330bc324ab46c2c

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Geophysics

1. L. Elkins‐Tanton
2. A. Morbidelli
3. D. Rubie
4. H. Palme
5. L. Stixrude
6. D. Frost
7. B. Wood
8. J. Wade

Citations in the corpus

• Core formation and the oxidation state of the Earth (2005, background): “7, the derived pressure– temperature conditions of equilibration, both for the single-stage process and for the dynamic process are, at constant oxygen fugacity (constant mantle Fe content) 700–1200 K above the peridotite liquidus ([34] [35]).”
• Thermodynamics of silicate liquids in the deep Earth (Invited) (2009, background): “…coefficient KFe=FePvMgL/(FeLMgPv)=0.4 consistent with experiments at lower pressure (Ito and Takahashi, 1987; Knittle, 1998; McFarlane et al., 1994; Tronnes and Frost, 2002), 2) that the influence of iron substitution on the density is similar in liquid and solid, and 3) the bulk iron content of…”
• Linked magma ocean solidification and atmospheric growth for Earth and Mars (2008, methodology): “…solidus used for Earth is fitted to experimental data on continental peridotite composition KLB-1 from (Takahashi, 1986; Herzberg and Zhang, 1996; Tronnes and Frost, 2002) and is given as: TEarthsol ¼ 1:160 10 7r3 þ 0:0014r2 6:382r þ 1:444 104 ð1Þ where r is radius in the terrestrial mantle in…”
• Accretion and differentiation of the terrestrial planets with implications for the compositions of early-formed Solar System bodies and accretion of water (2014, methodology): “We use a combination of liquidus/solidus temperatures of Herzberg and Zhang (1996), Trønnes and Frost (2002) and the “FeO corrected” liquidus and eutectic temperatures of Liebske and Frost (2012, Fig.”
• Solidus and liquidus profiles of chondritic mantle: Implication for melting of the Earth across its history (2011, background): “At low pressures, both solidus and liquidus curves are compatible with previous determinations using multi-anvil press (Litasov and Ohtani, 2002; Tronnes and Frost, 2002).”