Geometric flow properties of the germanate analog of forsterite
- 1 April 1978
- journal article
- Published by Elsevier in Tectonophysics
- Vol. 46 (1-2) , 187-196
- https://doi.org/10.1016/0040-1951(78)90113-0
Abstract
No abstract availableKeywords
This publication has 11 references indexed in Scilit:
- Mineralogy and chemistry of the Earth's mantle above 1000 kmGeophysical Journal International, 1977
- Steady state flow of rocksReviews of Geophysics, 1976
- Mechanisms of preferred orientations of olivine in tectonite peridotiteGeology, 1975
- Mechanisms of flow in naturally and experimentally deformed peridotitesAmerican Journal of Science, 1973
- A high-pressure, high-temperature apparatus for rock deformationInternational Journal of Rock Mechanics and Mining Sciences, 1970
- High Temperature Flow of Dunite and PeridotiteGSA Bulletin, 1970
- Syntectonic Recrystallization of Olivine and Modes of Flow in the Upper MantleGSA Bulletin, 1970
- The system Mg2SiO4Fe2SiO4 at high pressures and temperaturesPhysics of the Earth and Planetary Interiors, 1970
- Mechanisms of plastic deformation of olivineJournal of Geophysical Research, 1968
- Hydrolytic Weakening of Quartz and Other Silicates*Geophysical Journal of the Royal Astronomical Society, 1967