Seismic anisotropy evidence for dehydration embrittlement triggering intermediate-depth earthquakes
Abstract 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 proper...
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Formato: | article |
Lenguaje: | EN |
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Nature Portfolio
2017
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Acceso en línea: | https://doaj.org/article/93bf926994e8402faaa7678730fd29e6 |
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