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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
Hauptverfasser: Bykova, E., Bykov, M., Černok, A., Tidholm, J., Simak, S. I., Hellman, O., Belov, M. P., Abrikosov, I. A., Liermann, H.-P., Hanfland, M., Prakapenka, V. B., Prescher, C., Dubrovinskaia, N., Dubrovinsky, L.
Format: Artigo
Sprache:Inglês
Veröffentlicht: Nature Publishing Group UK 2018
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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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