Measurement of the melting curve of Mg0.9Fe0.1SiO3 at lower mantle conditions and its geophysical implications
- 10 October 1987
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research
- Vol. 92 (B11), 11437-11444
- https://doi.org/10.1029/jb092ib11p11437
Abstract
No abstract availableKeywords
This publication has 20 references indexed in Scilit:
- Garnet phase of MgSiO3 filling the pyroxene–ilmenite gap at very high temperatureNature, 1985
- Melting of peridotite to 14 GPa and the genesis of komatiiteNature, 1985
- Effect of high pressure on the melting relation of the Fe2SiO4-FeSiO3 system.Journal of Physics of the Earth, 1984
- Melting temperature distribution and fractionation in the lower mantlePhysics of the Earth and Planetary Interiors, 1983
- Melting of forsterite Mg2SiO4 up to 15 GPaPhysics of the Earth and Planetary Interiors, 1981
- The heat flow through oceanic and continental crust and the heat loss of the EarthReviews of Geophysics, 1980
- High Temperature Creep of Rock and Mantle ViscosityAnnual Review of Earth and Planetary Sciences, 1975
- Melting temperatures in the earth's mantleTectonophysics, 1972
- Temperatures in the earth's interiorJournal of Atmospheric and Terrestrial Physics, 1957
- A method of estimating the melting‐point gradient in the Earth's mantleEOS, Transactions American Geophysical Union, 1952