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Redox control on nitrogen isotope fractionation during planetary core formation
The present-day nitrogen isotopic compositions of Earth’s surficial ((15)N-enriched) and deep reservoirs ((15)N-depleted) differ significantly. This distribution can neither be explained by modern mantle degassing nor recycling via subduction zones. As the effect of planetary differentiation on the...
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| Опубликовано в: : | Proc Natl Acad Sci U S A |
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| Главные авторы: | , , , , , , , |
| Формат: | Artigo |
| Язык: | Inglês |
| Опубликовано: |
National Academy of Sciences
2019
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| Предметы: | |
| Online-ссылка: | https://ncbi.nlm.nih.gov/pmc/articles/PMC6642344/ https://ncbi.nlm.nih.gov/pubmed/31262822 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.1820719116 |
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