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Metastable silica high pressure polymorphs as structural proxies of deep Earth silicate melts
Modelling of processes involving deep Earth liquids requires information on their structures and compression mechanisms. However, knowledge of the local structures of silicates and silica (SiO(2)) melts at deep mantle conditions and of their densification mechanisms is still limited. Here we report...
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| Veröffentlicht in: | Nat Commun |
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| Hauptverfasser: | , , , , , , , , , , , , , |
| Format: | Artigo |
| Sprache: | Inglês |
| Veröffentlicht: |
Nature Publishing Group UK
2018
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| Schlagworte: | |
| Online Zugang: | https://ncbi.nlm.nih.gov/pmc/articles/PMC6237875/ https://ncbi.nlm.nih.gov/pubmed/30442940 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41467-018-07265-z |
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