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Reconciling metal–silicate partitioning and late accretion in the Earth
Highly siderophile elements (HSE), including platinum, provide powerful geochemical tools for studying planet formation. Late accretion of chondritic components to Earth after core formation has been invoked as the main source of mantle HSE. However, core formation could also have contributed to the...
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| 出版年: | Nat Commun |
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| 主要な著者: | , , , , , , |
| フォーマット: | Artigo |
| 言語: | Inglês |
| 出版事項: |
Nature Publishing Group UK
2021
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| 主題: | |
| オンライン･アクセス: | https://ncbi.nlm.nih.gov/pmc/articles/PMC8131616/ https://ncbi.nlm.nih.gov/pubmed/34006864 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41467-021-23137-5 |
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