Cargando…
Physical mechanisms of oceanic mantle earthquakes: Comparison of natural and experimental events
Because they provide information about the spatial distribution of brittle deformation, both seismologists and experimentalists use b-values to study earthquake populations. Here, we present the b-values for intermediate-depth intraslab earthquakes in the Pacific slab beneath the Tohoku and Hokkaido...
Autores principales: | Kita, Saeko, Ferrand, Thomas P. |
---|---|
Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
Nature Publishing Group UK
2018
|
Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6242829/ https://www.ncbi.nlm.nih.gov/pubmed/30451925 http://dx.doi.org/10.1038/s41598-018-35290-x |
Ejemplares similares
-
Dehydration-induced earthquakes identified in a subducted oceanic slab beneath Vrancea, Romania
por: Ferrand, Thomas P., et al.
Publicado: (2021) -
Electromagnetic exploration of the oceanic mantle
por: UTADA, Hisashi
Publicado: (2015) -
The mechanism of tidal triggering of earthquakes at mid-ocean ridges
por: Scholz, Christopher H., et al.
Publicado: (2019) -
Mantle Hg isotopic heterogeneity and evidence of oceanic Hg recycling into the mantle
por: Yin, Runsheng, et al.
Publicado: (2022) -
Coupled afterslip and transient mantle flow after the 2011 Tohoku earthquake
por: Muto, J., et al.
Publicado: (2019)