Dislocation-accommodated grain boundary sliding as the major deformation mechanism of olivine in the Earth’s upper mantle

Understanding the deformation mechanisms of olivine is important for addressing the dynamic processes in Earth’s upper mantle. It has been thought that dislocation creep is the dominant mechanism because of extrapolated laboratory data on the plasticity of olivine at pressures below 0.5 GPa. However...

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Detalles Bibliográficos
Autores principales: Ohuchi, Tomohiro, Kawazoe, Takaaki, Higo, Yuji, Funakoshi, Ken-ichi, Suzuki, Akio, Kikegawa, Takumi, Irifune, Tetsuo
Formato: Online Artículo Texto
Lenguaje:English
Publicado: American Association for the Advancement of Science 2015
Materias:
Research Articles
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4646795/
https://www.ncbi.nlm.nih.gov/pubmed/26601281
http://dx.doi.org/10.1126/sciadv.1500360

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4646795/
https://www.ncbi.nlm.nih.gov/pubmed/26601281
http://dx.doi.org/10.1126/sciadv.1500360

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