Melting experiment on natural lherzolite at 20 GPa: Formation of phase B coexisting with garnet
- 1 March 1986
- journal article
- Published by American Geophysical Union (AGU) in Geophysical Research Letters
- Vol. 13 (3), 181-184
- https://doi.org/10.1029/gl013i003p00181
Abstract
No abstract availableThis publication has 13 references indexed in Scilit:
- Incongruent melting of Mg2SiO4 at 20 GPaPhysics of the Earth and Planetary Interiors, 1985
- Stability of phase B, A hydrous magnesium silicate, to 2300°C at 20 GPAGeophysical Research Letters, 1985
- 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
- Generation of komatiite magma and gravitational differentiation in the deep upper mantleEarth and Planetary Science Letters, 1984
- Solidus and liquidus temperatures and mineralogies for anhydrous garnet-lherzolite to 15 GPaPhysics of the Earth and Planetary Interiors, 1983
- Melting of Various Silicates at Elevated PressuresPublished by Springer Science and Business Media LLC ,1982
- The system Mg2SiO4MgOH2O at high pressures and temperatures — Possible hydrous magnesian silicates in the mantle transition zonePhysics of the Earth and Planetary Interiors, 1980
- High-pressure phase equilibria in a garnet lherzolite, with special reference to Mg2+Fe2+ partitioning among constituent mineralsPhysics of the Earth and Planetary Interiors, 1979
- Melting relation of Fe2SiO4 up to about 200 kbar.Journal of Physics of the Earth, 1979