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Cold plumes trigger contamination of oceanic mantle wedges with continental crust-derived sediments: Evidence from chromitite zircon grains of eastern Cuban ophiolites
The origin of zircon grains, and other exotic minerals of typical crustal origin, in mantle-hosted ophiolitic chromitites are hotly debated. We report a population of zircon grains with ages ranging from Cretaceous (99 Ma) to Neoarchean (2750 Ma), separated from massive chromitite bodies hosted in t...
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Main Authors: | , , , , , , , , , , , , |
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Formato: | Artigo |
Idioma: | Inglês |
Publicado em: |
Elsevier
2018-11-01
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Colecção: | Geoscience Frontiers |
Acesso em linha: | http://www.sciencedirect.com/science/article/pii/S1674987117302165 |
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