Transformation mechanisms of San Carlos olivine to (MgFe)2SiO4 β-phase under subduction zone conditions
- 31 October 1994
- journal article
- Published by Elsevier BV in Physics of the Earth and Planetary Interiors
- Vol. 86 (1-3), 45-67
- https://doi.org/10.1016/0031-9201(94)05061-9
Abstract
No abstract availableKeywords
This publication has 28 references indexed in Scilit:
- FeMg interdiffusion in single crystal olivine at very high pressure and controlled oxygen fugacity: technological advances and initial data at 7 GPaPhysics of the Earth and Planetary Interiors, 1992
- Mechanisms of the transformations between the ?, ? and ? polymorphs of Mg2SiO4 at 15 GPaPhysics and Chemistry of Minerals, 1992
- Effects of H2O on the Disequilibrium Breakdown of Muscovite+QuartzJournal of Petrology, 1990
- Olivine‐modified spinel‐spinel transitions in the system Mg2SiO4‐Fe2SiO4: Calorimetric measurements, thermochemical calculation, and geophysical applicationJournal of Geophysical Research, 1989
- Stress dependence of the mechanism of the olivine–spinel transformationNature, 1989
- Olivine‐spinel transitions: Experimental and thermodynamic constraints and implications for the nature of the 400‐km seismic discontinuityJournal of Geophysical Research, 1987
- Layered convection induced by phase transitionsJournal of Geophysical Research, 1985
- The Diamond Cell and the Nature of the Earth's MantleAnnual Review of Earth and Planetary Sciences, 1979
- The quantitative analysis of thin specimensJournal of Microscopy, 1975
- The Earth's mantleEOS, Transactions American Geophysical Union, 1954