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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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| 發表在: | Nat Commun |
|---|---|
| Main Authors: | , , , , , , , , , |
| 格式: | Artigo |
| 語言: | Inglês |
| 出版: |
Nature Publishing Group UK
2018
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| 主題: | |
| 在線閱讀: | 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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