High temperature experiments on the elastic and anelastic behaviour of magmatic rocks
- 1 November 1985
- journal article
- Published by Elsevier in Physics of the Earth and Planetary Interiors
- Vol. 40 (3), 223-247
- https://doi.org/10.1016/0031-9201(85)90132-3
Abstract
No abstract availableThis publication has 45 references indexed in Scilit:
- Adiabats of quartz, coesite, olivine, and magnesium oxide to 50 kbar and 1000 K, and the adiabatic gradient in the Earth's mantleJournal of Geophysical Research, 1982
- Shear modulus and Q of forsterite and dunite near partial melting from forced-oscillation experimentsPhysics of the Earth and Planetary Interiors, 1982
- Absorption band Q model for the EarthJournal of Geophysical Research, 1982
- An investigation of the regional variations and frequency dependence of anelastic attenuation in the mantle under the United States in the 0.5-4 Hz bandGeophysical Journal International, 1982
- Preliminary reference Earth modelPhysics of the Earth and Planetary Interiors, 1981
- High-temperature anelasticity and elasticity of mantle peridotite — ReplyPhysics of the Earth and Planetary Interiors, 1980
- High-temperature anelasticity and elasticity of mantle peridotitePhysics of the Earth and Planetary Interiors, 1979
- The frequency dependence of Q in the Earth and implications for mantle rheology and Chandler wobbleGeophysical Journal International, 1979
- Electrical conductivity of olivine at high pressure and under controlled oxygen fugacityJournal of Geophysical Research, 1974
- The effect of ferric iron on the electrical conductivity of olivineEarth and Planetary Science Letters, 1973