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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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| Vydáno v: | Proc Natl Acad Sci U S A |
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| Hlavní autoři: | , , , |
| Médium: | Artigo |
| Jazyk: | Inglês |
| Vydáno: |
National Academy of Sciences
2019
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| Témata: | |
| On-line přístup: | 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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