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Melting curve of (Mg,Fe)SiO 3 perovskite to 96 GPa: Evidence for a structural transition in lower mantle melts
Author(s) -
Knittle Elise,
Jeanloz Raymond
Publication year - 1989
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/gl016i005p00421
Subject(s) - mantle (geology) , post perovskite , melting curve analysis , silicate , melting point , thermodynamics , mineralogy , extrapolation , transition zone , geology , perovskite (structure) , core–mantle boundary , materials science , analytical chemistry (journal) , crystallography , chemistry , geophysics , physics , polymerase chain reaction , mathematical analysis , biochemistry , mathematics , organic chemistry , composite material , gene , chromatography
The melting temperature of (Mg,Fe)SiO 3 perovskite, the dominant mineral phase of the Earth's lower mantle, has been measured to a pressure of 96 (±10) GPa. Below 60 GPa we find good agreement with the previous measurement of Heinz and Jeanloz [1987a], and above 60 GPa the melting curve of silicate perovskite has a small positive slope of 19.5 (±5.5) K/GPa. The melting point of (Mg 0.9 Fe 0.1 )SiO 3 perovskite is 3800 (±300) K at 96 GPa; by extrapolation to 136 GPa, it is 4500 (±500) K at the core‐mantle boundary. These values provide an upper limit to the geotherm through the solid mantle, and they are compatible with recent estimates of the temperature in the core being high (∼4500 K at the core‐mantle boundary). Our melting curve implies that the volume change on melting increases at 60 GPa from ΔV m = 0.0 (±0.2) cm³/mole to ΔV m ≅ 0.16 (±0.03) cm³/mole. We derive an equation of state for the melt from our data, and find that a highly coordinated structure is required to explain the molar volume of liquid (Mg,Fe)SiO 3 at pressures above ∼ 20 GPa.