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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Detaylı Bibliyografya
Yayımlandı:Nat Commun
Asıl Yazarlar: 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.
Materyal Türü: Artigo
Dil:Inglês
Baskı/Yayın Bilgisi: Nature Publishing Group UK 2018
Konular:
Article
Online Erişim: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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