Temperature and chemistry of the core-mantle boundary
- 1 March 1995
- journal article
- Published by Elsevier in Chemical Geology
- Vol. 120 (3-4), 199-205
- https://doi.org/10.1016/0009-2541(94)00138-x
Abstract
No abstract availableKeywords
This publication has 18 references indexed in Scilit:
- Constraints on the melting temperature of the lower mantle from high-pressure experiments on MgO and magnesioüstiteNature, 1994
- Melting of (Mg, Fe)SiO 3 -Perovskite to 625 Kilobars: Indication of a High Melting Temperature in the Lower MantleScience, 1993
- Temperatures in the Earth's core from melting-point measurements of iron at high static pressuresNature, 1993
- Geophysical inferences of thermal‐chemical structures in the lower mantleGeophysical Research Letters, 1993
- Sound velocities of MgO to very high compressionEarth and Planetary Science Letters, 1992
- On the scale of mantle heterogeneityPhysics of the Earth and Planetary Interiors, 1992
- Thermal expansivity in the lower mantleGeophysical Research Letters, 1992
- Partitioning of MgO, FeO, NiO, MnO and Cr2O3 between magnesian silicate perovskite and magnesiowüstite: implications for the origin of inclusions in diamond and the composition of the lower mantleEarth and Planetary Science Letters, 1992
- The system Fe-FeO revisitedPhysics and Chemistry of Minerals, 1990
- Thermodynamic parameters in the Earth as determined from seismic profilesGeophysical Journal International, 1981