Thermal expansion measurements at very high pressure, systematics, and a case for a chemically homogeneous mantle
- 1 November 1989
- journal article
- Published by American Geophysical Union (AGU) in Geophysical Research Letters
- Vol. 16 (11), 1347-1350
- https://doi.org/10.1029/gl016i011p01347
Abstract
No abstract availableThis publication has 26 references indexed in Scilit:
- Elasticity of MgSiO 3 in the Perovskite StructureScience, 1989
- Experimental determination of element partitioning between silicate perovskites, garnets and liquids: constraints on early differentiation of the mantleEarth and Planetary Science Letters, 1988
- Phase transformations in a harzburgite composition to 26 GPa: implications for dynamical behaviour of the subducting slabEarth and Planetary Science Letters, 1987
- Synthesis and Equation of State of (Mg,Fe) SiO 3 Perovskite to Over 100 GigapascalsScience, 1987
- First-principles theory for the equations of state of minerals at high pressures and temperatures: Application to MgOGeophysical Research Letters, 1985
- Some geophysical constraints on the chemical composition of the earth's lower mantleEarth and Planetary Science Letters, 1983
- Preliminary reference Earth modelPhysics of the Earth and Planetary Interiors, 1981
- Equation of state of sodium chloride up to 32 kbar and 500°C†Journal of Physics and Chemistry of Solids, 1980
- A new high-pressure phase of spinelEarth and Planetary Science Letters, 1978
- Equation of state of NaCl: Ultrasonic measurements to 8 kbar and 800°C and static lattice theoryJournal of Physics and Chemistry of Solids, 1972