Postspinel Phase of Forsterite and Evolution of the Earth's Mantle
- 1 February 1974
- journal article
- Published by Springer Nature in Nature
- Vol. 247 (5440) , 356-358
- https://doi.org/10.1038/247356a0
Abstract
No abstract availableThis publication has 16 references indexed in Scilit:
- The system MgO-FeO-SiO2 at high pressures and temperatures — phase equilibria and elastic propertiesTectonophysics, 1972
- PHASE TRANSFORMATIONS OF PURE Mg2SiO4 INTO A SPINEL STRUCTURE UNDER HIGH PRESSURES AND TEMPERATURESJournal of Physics of the Earth, 1972
- The system Mg2SiO4Fe2SiO4 at high pressures and temperaturesPhysics 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
- Seismic Waves Reflected from Discontinuities within Earth's Upper MantleScience, 1969
- Phase Changes in the Upper MantleScience, 1967
- The viscosity of the lower mantleJournal of Geophysical Research, 1966
- Olivine-spinel transition in the system Mg2SiO4-Fe2SiO4 at 800°CEarth and Planetary Science Letters, 1966
- Upper mantle structure of western North America from apparent velocities ofPwavesJournal of Geophysical Research, 1965
- Elasticity and constitution of the Earth's interiorJournal of Geophysical Research, 1952