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Iron diapirs entrain silicates to the core and initiate thermochemical plumes
Segregation of the iron core from rocky silicates is a massive evolutionary event in planetary accretion, yet the process of metal segregation remains obscure, due to obstacles in simulating the extreme physical properties of liquid iron and silicates at finite length scales. We present new experime...
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| Опубликовано в: : | Nat Commun |
|---|---|
| Главные авторы: | , , , , , , , , , |
| Формат: | Artigo |
| Язык: | Inglês |
| Опубликовано: |
Nature Publishing Group UK
2018
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| Предметы: | |
| Online-ссылка: | https://ncbi.nlm.nih.gov/pmc/articles/PMC5754369/ https://ncbi.nlm.nih.gov/pubmed/29302028 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41467-017-02503-2 |
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