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Evidence for Fe-Si-O liquid immiscibility at deep Earth pressures

Seismic observations suggest that the uppermost region of Earth’s liquid outer core is buoyant, with slower velocities than the bulk outer core. One possible mechanism for the formation of a stably stratified layer is immiscibility in molten iron alloy systems, which has yet to be demonstrated at co...

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Detalhes bibliográficos
Publicado no:Proc Natl Acad Sci U S A
Main Authors: Arveson, Sarah M., Deng, Jie, Karki, Bijaya B., Lee, Kanani K. M.
Formato: Artigo
Idioma:Inglês
Publicado em: National Academy of Sciences 2019
Assuntos:
Acesso em linha:https://ncbi.nlm.nih.gov/pmc/articles/PMC6534994/
https://ncbi.nlm.nih.gov/pubmed/31068466
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.1821712116
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