Anisotropic growth in the olivine-spinel transformation of Mg2GeO4 under nonhydrostatic stress
- 1 October 1984
- journal article
- Published by Elsevier in Tectonophysics
- Vol. 108 (3-4) , 299-322
- https://doi.org/10.1016/0040-1951(84)90241-5
Abstract
No abstract availableKeywords
This publication has 27 references indexed in Scilit:
- Olivine to spinel transformation in Mg2SiO4 via faulted structuresNature, 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
- Exsolution of Ca-clinopyroxene from orthopyroxene aided by deformationPhysics and Chemistry of Minerals, 1981
- Mechanical and thermodynamic constraints on fluid distribution in partial meltsJournal of Geophysical Research, 1979
- High-pressure phase equilibria in a garnet lherzolite, with special reference to Mg2+Fe2+ partitioning among constituent mineralsPhysics of the Earth and Planetary Interiors, 1979
- The orthoenstatite to clinoenstatite transformation by shearing and reversion by annealing: Mechanism and potential applicationsContributions to Mineralogy and Petrology, 1975
- The thermodynamic effect of shear stress on the ortho-clino inversion in enstatite and other coherent phase transitions characterized by a finite simple shearContributions to Mineralogy and Petrology, 1970
- The α-β Inversion in quartz: A coherent phase transition under nonhydrostatic stressJournal of Geophysical Research, 1969
- The olivine-spinel transition in Fe2SiO4and Ni2SiO4Journal of Geophysical Research, 1965