Elasticity of single‐crystal forsterite measured to 1700 K
- 10 May 1989
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research
- Vol. 94 (B5), 5895-5906
- https://doi.org/10.1029/jb094ib05p05895
Abstract
No abstract availableThis publication has 32 references indexed in Scilit:
- Transition region of the Earth's upper mantleNature, 1986
- A mineral physics test of a pyrolite mantleGeophysical Research Letters, 1985
- Composition of the upper mantle: Geophysical tests of two petrological modelsGeophysical Research Letters, 1984
- Elastic properties of a single-crystal forsterite Mg2SiO4, up to 1,200 KPhysics and Chemistry of Minerals, 1983
- Thermodynamics and lattice vibrations of minerals: 1. Mineral heat capacities and their relationships to simple lattice vibrational modelsReviews of Geophysics, 1979
- The elastic constants of Mn2SiO4, Fe2SiO4 and Co2SiO4, and the elastic properties of olivine group minerals at high temperature.Journal of Physics of the Earth, 1979
- Elastic properties of garnet solid-solution seriesPhysics of the Earth and Planetary Interiors, 1978
- Temperature variation of elastic constants of single-crystal forsterite between -190.DEG. and 400.DEG.C.Journal of Physics of the Earth, 1977
- Thermal expansion of periclase and olivine, and their anharmonic properties.Journal of Physics of the Earth, 1975
- High‐Temperature Elasticity and Expansivity of Forsterite and SteatiteJournal of the American Ceramic Society, 1967