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...

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Detalles Bibliográficos
Autores principales: Wang, Jian, Zhao, Dapeng, Yao, Zhenxing
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2017
Materias:
Article
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

Internet

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

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