The system Mg2SiO4Fe2SiO4 at high pressures and temperatures
- 1 January 1970
- journal article
- Published by Elsevier in Physics of the Earth and Planetary Interiors
- Vol. 3, 89-108
- https://doi.org/10.1016/0031-9201(70)90046-4
Abstract
No abstract availableThis publication has 44 references indexed in Scilit:
- High-pressure decomposition of the system FeSiO3MgSiO3Physics of the Earth and Planetary Interiors, 1970
- Crystal structures of high pressure modifications of Mn2GeO4 and Co2SiO4Physics of the Earth and Planetary Interiors, 1970
- (Mg,Fe)2SiO4 spinel in a meteoritePhysics of the Earth and Planetary Interiors, 1970
- Split sphere high pressure vessel and phase equilibrium relation in the system Mg2SiO4Fe2SiO4Physics of the Earth and Planetary Interiors, 1970
- Crystal structure of β-Mg2SiO4: crystal-chemical and geophysical implicationsPhysics of the Earth and Planetary Interiors, 1970
- Apparatus for phase transformation studies at high pressures and temperaturesPhysics of the Earth and Planetary Interiors, 1968
- Phase transformations in the mantleEarth and Planetary Science Letters, 1968
- Density distribution and constitution of the mantleReviews of Geophysics, 1964
- High pressure studies of the system Mg 2 GeO 4 Mg 2 SiO 4 with special reference to the olivine-spinel traansitionAmerican Journal of Science, 1960
- A simple apparatus for high pressures and temperaturesAmerican Journal of Science, 1956