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Sulfur and lead isotopic evidence of relic Archean sediments in the Pitcairn mantle plume
The isotopic diversity of oceanic island basalts (OIB) is usually attributed to the influence, in their sources, of ancient material recycled into the mantle, although the nature, age, and quantities of this material remain controversial. The unradiogenic Pb isotope signature of the enriched mantle...
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| Publicat a: | Proc Natl Acad Sci U S A |
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| Autors principals: | , , , , |
| Format: | Artigo |
| Idioma: | Inglês |
| Publicat: |
National Academy of Sciences
2016
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| Matèries: | |
| Accés en línia: | https://ncbi.nlm.nih.gov/pmc/articles/PMC5135331/ https://ncbi.nlm.nih.gov/pubmed/27791057 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.1523805113 |
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