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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Detalles Bibliográficos
Autores principales: 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: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2018
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6237875/
https://www.ncbi.nlm.nih.gov/pubmed/30442940
http://dx.doi.org/10.1038/s41467-018-07265-z

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6237875/
https://www.ncbi.nlm.nih.gov/pubmed/30442940
http://dx.doi.org/10.1038/s41467-018-07265-z

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