This is a Preprint and has not been peer reviewed. The published version of this Preprint is available: https://doi.org/10.1016/j.pepi.2018.12.004. This is version 1 of this Preprint.
This is a Preprint and has not been peer reviewed. The published version of this Preprint is available: https://doi.org/10.1016/j.pepi.2018.12.004. This is version 1 of this Preprint.
Dislocation glide is an important contributor to the rheology of olivine under conditions of high stress and low to moderate temperature, such as occur in mantle wedges. Interactions between point defects and dislocation core may alter the Peierls stress,
https://doi.org/10.31223/osf.io/nj5mf
Condensed Matter Physics, Earth Sciences, Geophysics and Seismology, Mineral Physics, Physical Sciences and Mathematics, Physics
forsterite, dislocation, cation vacancies, Peierls-Nabarro modeling, Peierls stress
Published: 2018-07-26 19:59
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