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Arc-like magmas generated by mélange-peridotite interaction in the mantle wedge
The mechanisms of transfer of crustal material from the subducting slab to the overlying mantle wedge are still debated. Mélange rocks, formed by mixing of sediments, oceanic crust, and ultramafics along the slab-mantle interface, are predicted to ascend as diapirs from the slab-top and transfer the...
| Autores principales: | , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
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Nature Publishing Group UK
2018
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| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6054672/ https://www.ncbi.nlm.nih.gov/pubmed/30030428 http://dx.doi.org/10.1038/s41467-018-05313-2 |