Chargement en cours...

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...

Description complète

Enregistré dans:
Détails bibliographiques
Publié dans:Nat Commun
Auteurs principaux: Codillo, E. A., Le Roux, V., Marschall, H. R.
Format: Artigo
Langue:Inglês
Publié: Nature Publishing Group UK 2018
Sujets:
Accès en ligne:https://ncbi.nlm.nih.gov/pmc/articles/PMC6054672/
https://ncbi.nlm.nih.gov/pubmed/30030428
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41467-018-05313-2
Tags: Ajouter un tag
Pas de tags, Soyez le premier à ajouter un tag!