Evidence for a serpentinized plate interface favouring continental subduction

The dynamics of continental subduction is largely controlled by the rheological properties of rocks involved along the subduction channel. Serpentinites have low viscosity at geological strain rates. However, compelling geophysical evidence of a serpentinite channel during continental subduction is...

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Detalles Bibliográficos
Autores principales: Zhao, Liang, Malusà, Marco G., Yuan, Huaiyu, Paul, Anne, Guillot, Stéphane, Lu, Yang, Stehly, Laurent, Solarino, Stefano, Eva, Elena, Lu, Gang, Bodin, Thomas
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2020
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7195360/
https://www.ncbi.nlm.nih.gov/pubmed/32358508
http://dx.doi.org/10.1038/s41467-020-15904-7

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7195360/
https://www.ncbi.nlm.nih.gov/pubmed/32358508
http://dx.doi.org/10.1038/s41467-020-15904-7

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