High-pressure, high-temperature Raman spectroscopy of Ca2GeO4 (olivine form): some insights on anharmonicity
- 1 December 1989
- journal article
- Published by Elsevier in Physics of the Earth and Planetary Interiors
- Vol. 58 (2-3), 141-154
- https://doi.org/10.1016/0031-9201(89)90050-2
Abstract
No abstract availableKeywords
This publication has 18 references indexed in Scilit:
- Temperature and pressure derivatives of elastic constants with application to the mantleJournal of Geophysical Research, 1988
- Single-crystal absorption and reflection infrared spectroscopy of forsterite and fayalitePhysics and Chemistry of Minerals, 1987
- Comparison of the raman microprobe spectra of (Mg, Fe)2SiO4 and Mg2GeO4 with olivine and spinel structuresPhysics and Chemistry of Minerals, 1986
- The crystal structure of forsterite Mg2SiO4 under high pressure up to 149 kbZeitschrift für Kristallographie - Crystalline Materials, 1985
- LASER RAMAN MICROPROBING TECHNIQUESLe Journal de Physique Colloques, 1984
- Anharmonicity of three minerals at high temperature: Forsterite, fayalite, and periclaseJournal of Geophysical Research, 1983
- Raman spectra of olivine up to 65 kilobarsJournal of Geophysical Research, 1982
- Infrared spectra of olivine polymorphs: ?, ? phase and spinelPhysics and Chemistry of Minerals, 1980
- Elasticity of Olivine (α), Beta(β), and Spinel (γ) Polymorphs of Germanates and SilicatesGeophysical Journal of the Royal Astronomical Society, 1975
- Anharmonicity in silicate crystals: Temperature dependence of Au type vibrational modes in ZrSiO4 and LiAlSi2O6Journal of Physics and Chemistry of Solids, 1973