Iron diapirs entrain silicates to the core and initiate thermochemical plumes

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 an...

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Autores principales: 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
Formato: article
Lenguaje:EN
Publicado: Nature Portfolio 2018
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Acceso en línea:https://doaj.org/article/89cf21a977f8406abb9f65f0373fa600
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