Light oxygen isotopes in mantle-derived magmas reflect assimilation of sub-continental lithospheric mantle material

Oxygen isotope ratios in mantle-derived magmas that differ from typical mantle values are generally attributed to crustal contamination, deeply subducted crustal material in the mantle source or primordial heterogeneities. Here we provide an alternative view for the origin of light oxygen-isotope si...

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Detalles Bibliográficos
Autores principales: Xu, Jing-Yao, Giuliani, Andrea, Li, Qiu-Li, Lu, Kai, Melgarejo, Joan Carles, Griffin, William L.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2021
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8563987/
https://www.ncbi.nlm.nih.gov/pubmed/34728640
http://dx.doi.org/10.1038/s41467-021-26668-z

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8563987/
https://www.ncbi.nlm.nih.gov/pubmed/34728640
http://dx.doi.org/10.1038/s41467-021-26668-z

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