A comparison of the creep properties of pure forsterite and iron-bearing olivine
- 1 July 1977
- journal article
- research article
- Published by Elsevier in Tectonophysics
- Vol. 40 (3-4) , T15-T18
- https://doi.org/10.1016/0040-1951(77)90063-4
Abstract
No abstract availableThis publication has 4 references indexed in Scilit:
- Plastic flow of oriented single crystals of olivine: 2. Observations and interpretations of the dislocation structuresJournal of Geophysical Research, 1977
- Low-stress high-temperature creep in olivine single crystalsJournal of Geophysical Research, 1974
- Stability field of olivine with respect to oxidation and reductionJournal of Geophysical Research, 1974
- High Temperature Flow of Dunite and PeridotiteGSA Bulletin, 1970