The nature and significance of stacking faults in wadsleyite, natural β-(Mg, Fe)2SiO4 from the Peace River meteorite
- 1 September 1983
- journal article
- Published by Elsevier in Physics of the Earth and Planetary Interiors
- Vol. 33 (2) , 137-147
- https://doi.org/10.1016/0031-9201(83)90146-2
Abstract
No abstract availableKeywords
This publication has 15 references indexed in Scilit:
- Transmission electron microscope observation of α, β and γ (Mg, Fe)2SiO4 in shocked meteorites: planar defects and polymorphic transitionsPhysics of the Earth and Planetary Interiors, 1983
- The system NiAl2O4Ni2SiO4 at high pressures and temperatures: Spinelloids with spinel-related structuresJournal of Solid State Chemistry, 1982
- A spinel to β-phase transformation mechanism in (Mg,Fe)2SiO4Nature, 1982
- High-pressure (Mg, Fe)2SiO4 phases in the Tenham chondritic meteoriteNature, 1979
- Role of Phase Transitions in a Dynamic MantleGeophysical Journal of the Royal Astronomical Society, 1975
- Phase transformations and mantle dynamicsEarth and Planetary Science Letters, 1972
- Crystal structures of high pressure modifications of Mn2GeO4 and Co2SiO4Physics of the Earth and Planetary Interiors, 1970
- Crystal structure of β-Mg2SiO4: crystal-chemical and geophysical implicationsPhysics of the Earth and Planetary Interiors, 1970
- High-pressure transformation of FeSiO3 pyroxene to spinel plus stishoviteEarth and Planetary Science Letters, 1966
- Intensity Profiles for Fringe Patterns Due to Planar Interfaces as Observed by Electron MicroscopyPhysica Status Solidi (b), 1965