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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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| Publicado no: | Nat Commun |
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| Main Authors: | , , , , , , , , , , |
| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado em: |
Nature Publishing Group UK
2017
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| Assuntos: | |
| Acesso em linha: | https://ncbi.nlm.nih.gov/pmc/articles/PMC5736553/ https://ncbi.nlm.nih.gov/pubmed/29259168 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41467-017-02273-x |
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