The rheology of faults triggered by the olivine-spinel transformation in Mg2GeO4 and its implications for the mechanism of deep-focus earthquakes
- 1 September 1993
- journal article
- Published by Elsevier in Journal of Structural Geology
- Vol. 15 (9-10) , 1249-1256
- https://doi.org/10.1016/0191-8141(93)90167-9
Abstract
No abstract availableKeywords
This publication has 11 references indexed in Scilit:
- Acoustic emissions produced by anticrack faulting during the olivine→spinel transformationGeophysical Research Letters, 1992
- Mantle Phase Changes and Deep-Earthquake Faulting in Subducting LithosphereScience, 1991
- Faulting associated with the olivine to spinel transformation in Mg2GeO4 and its implications for deep‐focus earthquakesJournal of Geophysical Research, 1991
- Anticrack-associated faulting at very high pressure in natural olivineNature, 1990
- Frictional behavior and constitutive modeling of simulated fault gougeJournal of Geophysical Research, 1990
- A new self-organizing mechanism for deep-focus earthquakesNature, 1989
- Stress dependence of the mechanism of the olivine–spinel transformationNature, 1989
- Particle-size distribution and microstructures within simulated fault gougeJournal of Structural Geology, 1989
- Localized polymorphic phase transformations in high‐pressure faults and applications to the physical mechanism of deep earthquakesJournal of Geophysical Research, 1987
- Friction of rocksPure and Applied Geophysics, 1978