Stress dependence of recrystallized-grain and subgrain size in olivine
- 1 December 1980
- journal article
- Published by Elsevier in Tectonophysics
- Vol. 70 (1-2), 39-61
- https://doi.org/10.1016/0040-1951(80)90020-7
Abstract
No abstract availableKeywords
This publication has 25 references indexed in Scilit:
- Rheology of the upper mantle: Inferences from peridotite xenolithsTectonophysics, 1980
- Experimental deformation of diopside and websteriteTectonophysics, 1978
- Plastic flow of oriented single crystals of olivine: 2. Observations and interpretations of the dislocation structuresJournal of Geophysical Research, 1977
- Steady state flow of rocksReviews of Geophysics, 1976
- High‐temperature flow of rocksReviews of Geophysics, 1975
- Sheared Iherzolites: From the point of view of rock mechanicsGeology, 1975
- Recovery and recrystallization during high temperature deformation of α-ironMetallurgical Transactions, 1973
- High Temperature Flow of Dunite and PeridotiteGSA Bulletin, 1970
- Syntectonic Recrystallization of Olivine and Modes of Flow in the Upper MantleGSA Bulletin, 1970
- The flow stress of polycrystalline aluminiumPhilosophical Magazine, 1957