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Iron isotopic fractionation between silicate mantle and metallic core at high pressure
The +0.1‰ elevated (56)Fe/(54)Fe ratio of terrestrial basalts relative to chondrites was proposed to be a fingerprint of core-mantle segregation. However, the extent of iron isotopic fractionation between molten metal and silicate under high pressure–temperature conditions is poorly known. Here we s...
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| Опубликовано в: : | Nat Commun |
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| Главные авторы: | , , , , , , , , , |
| Формат: | Artigo |
| Язык: | Inglês |
| Опубликовано: |
Nature Publishing Group
2017
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| Предметы: | |
| Online-ссылка: | https://ncbi.nlm.nih.gov/pmc/articles/PMC5321738/ https://ncbi.nlm.nih.gov/pubmed/28216664 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/ncomms14377 |
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