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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Detalles Bibliográficos
Autores principales: Fleck, J. R., Rains, C. L., Weeraratne, D. S., Nguyen, C. T., Brand, D. M., Klein, S. M., McGehee, J. M., Rincon, J. M., Martinez, C., Olson, P. L.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2018
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5754369/
https://www.ncbi.nlm.nih.gov/pubmed/29302028
http://dx.doi.org/10.1038/s41467-017-02503-2

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5754369/
https://www.ncbi.nlm.nih.gov/pubmed/29302028
http://dx.doi.org/10.1038/s41467-017-02503-2

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