| Autor: |
J. R. Fleck, C. L. Rains, D. S. Weeraratne, C. T. Nguyen, D. M. Brand, S. M. Klein, J. M. McGehee, J. M. Rincon, C. Martinez, P. L. Olson |
| Jazyk: |
angličtina |
| Rok vydání: |
2018 |
| Předmět: |
|
| Zdroj: |
Nature Communications, Vol 9, Iss 1, Pp 1-12 (2018) |
| Druh dokumentu: |
article |
| ISSN: |
2041-1723 |
| DOI: |
10.1038/s41467-017-02503-2 |
| Popis: |
During planetary formation segregation of an iron core from rocky silicates takes place. Here, the authors use analogue fluid experiments show that iron diapirs entrain volatiles and silicates to the Earth’s core and initiate buoyant thermochemical plumes to reoxidize and hydrate the upper mantle and atmosphere. |
| Databáze: |
Directory of Open Access Journals |
| Externí odkaz: |
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