Partial melting of rocks observed by the sound velocity method and the possibility of a quasi-dry low velocity zone in the upper mantle
- 1 June 1989
- journal article
- Published by Elsevier in Physics of the Earth and Planetary Interiors
- Vol. 55 (3-4) , 306-312
- https://doi.org/10.1016/0031-9201(89)90078-2
Abstract
No abstract availableKeywords
This publication has 14 references indexed in Scilit:
- Rheology and structure of olivine‐basalt partial meltsJournal of Geophysical Research, 1986
- The effects of frequency on the elastic wave velocity in rocks at high temperatures under pressureTectonophysics, 1986
- The Generation and Compaction of Partially Molten RockJournal of Petrology, 1984
- Compressional and shear wave velocities of igneous rocks and volcanic glasses to 900° C and 20 kbarTectonophysics, 1981
- Velocity and attenuation in partially molten rocksJournal of Geophysical Research, 1980
- Regional upper mantle S-velocity models from phase velocities of great-circle Rayleigh wavesGeophysical Journal International, 1980
- Viscoelastic properties of fluid-saturated cracked solidsJournal of Geophysical Research, 1977
- Pyroxene geothermsJournal of Geophysical Research, 1975
- The elastic constants of single-crystal orthopyroxeneJournal of Geophysical Research, 1969
- Elastic moduli, pressure derivatives, and temperature derivatives of single-crystal olivine and single-crystal forsteriteJournal of Geophysical Research, 1969