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Oxygen isotope (δ(18)O, Δ′(17)O) insights into continental mantle evolution since the Archean

Oxygen isotopic ratios are largely homogenous in the bulk of Earth’s mantle but are strongly fractionated near the Earth’s surface, thus these are robust indicators of recycling of surface materials to the mantle. Here we document a subtle but significant ~0.2‰ temporal decrease in δ(18)O in the sha...

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Detalles Bibliográficos
Autores principales:	Bindeman, Ilya N., Ionov, Dmitri A., Tollan, Peter M. E., Golovin, Alexander V.
Formato:	Online Artículo Texto
Lenguaje:	English
Publicado:	Nature Publishing Group UK 2022
Materias:	Article
Acceso en línea:	https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9253152/ https://www.ncbi.nlm.nih.gov/pubmed/35788136 http://dx.doi.org/10.1038/s41467-022-31586-9

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