Lower plate serpentinite diapirism in the Calabrian Arc subduction complex

Mantle-derived serpentinites have been detected at magma-poor rifted margins and above subduction zones, where they are usually produced by fluids released from the slab to the mantle wedge. Here we show evidence of a new class of serpentinite diapirs within the external subduction system of the Cal...

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Detalles Bibliográficos
Autores principales: Polonia, A., Torelli, L., Gasperini, L., Cocchi, L., Muccini, F., Bonatti, E., Hensen, C., Schmidt, M., Romano, S., Artoni, A., Carlini, M.
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/PMC5736553/
https://www.ncbi.nlm.nih.gov/pubmed/29259168
http://dx.doi.org/10.1038/s41467-017-02273-x

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5736553/
https://www.ncbi.nlm.nih.gov/pubmed/29259168
http://dx.doi.org/10.1038/s41467-017-02273-x

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