Cargando…
In situ X-ray and acoustic observations of deep seismic faulting upon phase transitions in olivine
The activity of deep-focus earthquakes, which increases with depth from ~400 km to a peak at ~600 km, is enigmatic, because conventional brittle failure is unlikely to occur at elevated pressures. It becomes increasingly clear that pressure-induced phase transitions of olivine are responsible for th...
Autores principales: | Ohuchi, Tomohiro, Higo, Yuji, Tange, Yoshinori, Sakai, Takeshi, Matsuda, Kohei, Irifune, Tetsuo |
---|---|
Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
Nature Publishing Group UK
2022
|
Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9477848/ https://www.ncbi.nlm.nih.gov/pubmed/36109510 http://dx.doi.org/10.1038/s41467-022-32923-8 |
Ejemplares similares
-
Dislocation-accommodated grain boundary sliding as the major deformation mechanism of olivine in the Earth’s upper mantle
por: Ohuchi, Tomohiro, et al.
Publicado: (2015) -
Ultrafast olivine-ringwoodite transformation during shock compression
por: Okuchi, Takuo, et al.
Publicado: (2021) -
Sintering Behaviour of Waste Olivine and Olivine/Alumina Blends
por: Furlani, Erika, et al.
Publicado: (2014) -
Viscosity of bridgmanite determined by in situ stress and strain measurements in uniaxial deformation experiments
por: Tsujino, Noriyoshi, et al.
Publicado: (2022) -
Effect of water on seismic attenuation of the upper mantle: The origin of the sharp lithosphere–asthenosphere boundary
por: Liu, Chao, et al.
Publicado: (2023)