An olivine to beta phase transformation mechanism Mg2SiO4
- 1 January 1991
- journal article
- Published by American Geophysical Union (AGU) in Geophysical Research Letters
- Vol. 18 (1), 89-92
- https://doi.org/10.1029/90gl02719
Abstract
No abstract availableThis publication has 16 references indexed in Scilit:
- Hot‐pressing and characterization of polycrystals of β‐Mg2SiO4, for acoustic velocity measurementsGeophysical Research Letters, 1990
- The system Mg2SiO4‐Fe2SiO4 at high pressures and temperatures: Precise determination of stabilities of olivine, modified spinel, and spinelJournal of Geophysical Research, 1989
- Stress dependence of the mechanism of the olivine–spinel transformationNature, 1989
- Mechanism of the olivine-spinel transformation in Co2SiO4Physics and Chemistry of Minerals, 1988
- Investigation of the mechanism of the olivine‐spinel transition in fayalite by synchrotron radiationJournal of Geophysical Research, 1983
- The nature and significance of stacking faults in wadsleyite, natural β-(Mg, Fe)2SiO4 from the Peace River meteoritePhysics of the Earth and Planetary Interiors, 1983
- Mechanism of the olivine to spinel phase transformation in Ni2SiO4Geophysical Research Letters, 1983
- On the mechanism of the olivine-spinel phase transformationPhysics of the Earth and Planetary Interiors, 1982
- A spinel to β-phase transformation mechanism in (Mg,Fe)2SiO4Nature, 1982
- Olivine glass and spinel formed in a laser heated, diamond-anvil high pressure cellNature, 1980