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Seismic anisotropy evidence for dehydration embrittlement triggering intermediate-depth earthquakes
It has been proposed that dehydration embrittlement of hydrous materials can trigger intermediate-depth earthquakes and form a double seismic zone in a subducting slab. Seismic anisotropy may provide a possible insight into intermediate-depth intraslab seismicity, because anisotropic properties of m...
| Autores principales: | , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
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Nature Publishing Group UK
2017
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| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5453959/ https://www.ncbi.nlm.nih.gov/pubmed/28572682 http://dx.doi.org/10.1038/s41598-017-02563-w |