Stability relation of (Mg,Fe)SiO3 garnets, major constituents in the Earth's interior
- 1 April 1986
- journal article
- Published by Elsevier in Earth and Planetary Science Letters
- Vol. 77 (3-4), 399-408
- https://doi.org/10.1016/0012-821x(86)90149-4
Abstract
No abstract availableThis publication has 17 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
- Effect of high pressure on the melting relation of the Fe2SiO4-FeSiO3 system.Journal of Physics of the Earth, 1984
- Majorite: Vibrational and compressional properties of a high‐pressure phaseJournal of Geophysical Research, 1981
- Electron petrography of shock-produced veins in the Tenham chondriteContributions to Mineralogy and Petrology, 1979
- Melting relation of Fe2SiO4 up to about 200 kbar.Journal of Physics of the Earth, 1979
- Pyroxene-garnet solid-solution equilibria in the systems Mg4Si4O12Mg3Al2Si3O12 and Fe4Si4O12Fe3Al2Si3O12 at high pressures and temperaturesPhysics of the Earth and Planetary Interiors, 1977
- (Mg,Fe)2SiO4 spinel in a meteoritePhysics of the Earth and Planetary Interiors, 1970
- High-pressure transformations in pyroxenesEarth and Planetary Science Letters, 1966