Mineral physics constraints on the chemical composition of the Earth's lower mantle
- 30 September 1994
- journal article
- Published by Elsevier in Physics of the Earth and Planetary Interiors
- Vol. 85 (3-4) , 273-292
- https://doi.org/10.1016/0031-9201(94)90118-x
Abstract
No abstract availableKeywords
This publication has 53 references indexed in Scilit:
- A thermodynamic theory of the Gr neisen ratio at extreme conditions: MgO as an examplePhysics and Chemistry of Minerals, 1993
- High‐temperature elastic constant data on minerals relevant to geophysicsReviews of Geophysics, 1992
- Thermal expansivity versus pressure at constant temperature: A re‐examinationGeophysical Research Letters, 1990
- Measurement of elastic constants of mantle-related minerals at temperatures up to 1800 KPhysics of the Earth and Planetary Interiors, 1989
- Temperature and pressure derivatives of elastic constants with application to the mantleJournal of Geophysical Research, 1988
- Mineralogy and composition of the upper mantleGeophysical Research Letters, 1984
- The Earth as a Planet: Paradigms and ParadoxesScience, 1984
- Chemical composition of the mantleJournal of Geophysical Research, 1983
- Composition of the Earth's MantleGeophysical Journal International, 1961
- Elasticity and constitution of the Earth's interiorJournal of Geophysical Research, 1952