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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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Publicado en:Nat Commun
Main Authors: 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.
Formato: Artigo
Idioma:Inglês
Publicado: Nature Publishing Group UK 2018
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Acceso en liña: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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