Transmission electron microscope observation of α, β and γ (Mg, Fe)2SiO4 in shocked meteorites: planar defects and polymorphic transitions
- 31 August 1983
- journal article
- Published by Elsevier BV in Physics of the Earth and Planetary Interiors
- Vol. 33 (1), 31-44
- https://doi.org/10.1016/0031-9201(83)90005-5
Abstract
No abstract availableKeywords
This publication has 26 references indexed in Scilit:
- Structures related to those of spinel and theβ-phase, and a possible mechanism for the transformation olivine ↔ spinelZeitschrift für Kristallographie, 1982
- The Diamond Cell and the Nature of the Earth's MantleAnnual Review of Earth and Planetary Sciences, 1979
- Electron microscopy of some stony meteoritesPhilosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences, 1977
- Composition of the Mantle and CoreAnnual Review of Earth and Planetary Sciences, 1977
- Dissociation of dislocations in spinels (Al2O3) 1.8MgOJournal de Physique Lettres, 1974
- Pressure dependence of single crystal elastic constants and anharmonic properties of wurtziteJournal of Physics and Chemistry of Solids, 1973
- (Mg,Fe)2SiO4 spinel in a meteoritePhysics of the Earth and Planetary Interiors, 1970
- Ringwoodite, Natural (Mg,Fe)2SiO4 Spinel in the Tenham MeteoriteNature, 1969
- Deformation of olivine in stony meteoritesJournal of Geophysical Research, 1968
- Intensity Profiles for Fringe Patterns Due to Planar Interfaces as Observed by Electron MicroscopyPhysica Status Solidi (b), 1965