Elasticity of forsterite to 16 GPa and the composition of the upper mantle
- 1 November 1995
- journal article
- letter
- Published by Springer Nature in Nature
- Vol. 378 (6553) , 170-173
- https://doi.org/10.1038/378170a0
Abstract
No abstract availableKeywords
This publication has 25 references indexed in Scilit:
- Seismic heterogeneity in the upper mantleJournal of Geophysical Research, 1994
- Petrology, elasticity, and composition of the mantle transition zoneJournal of Geophysical Research, 1992
- Pressure Dependence of Elastic Wave Velocity for β-Mg 2 SiO 4 and the Composition of the Earth's MantleScience, 1990
- Olivine‐modified spinel‐spinel transitions in the system Mg2SiO4‐Fe2SiO4: Calorimetric measurements, thermochemical calculation, and geophysical applicationJournal of Geophysical Research, 1989
- Elasticity of single‐crystal forsterite measured to 1700 KJournal of Geophysical Research, 1989
- Seismic velocities in mantle minerals and the mineralogy of the upper mantleJournal of Geophysical Research, 1989
- The 400-km seismic discontinuity and the proportion of olivine in the Earth's upper mantleNature, 1986
- A mineral physics test of a pyrolite mantleGeophysical Research Letters, 1985
- Elastic moduli, pressure derivatives, and temperature derivatives of single-crystal olivine and single-crystal forsteriteJournal of Geophysical Research, 1969
- Elastic constants of single-crystal forsterite as a function of temperature and pressureJournal of Geophysical Research, 1969