The post-stishovite phase transition in hydrous alumina-bearing SiO(2) in the lower mantle of the earth

Silica is the most abundant oxide component in the Earth mantle by weight, and stishovite, the rutile-structured (P4(2)/mnm) high-pressure phase with silica in six coordination by oxygen, is one of the main constituents of the basaltic layer of subducting slabs. It may also be present as a free phas...

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Hlavní autoři: Lakshtanov, Dmitry L., Sinogeikin, Stanislav V., Litasov, Konstantin D., Prakapenka, Vitali B., Hellwig, Holger, Wang, Jingyun, Sanches-Valle, Carmen, Perrillat, Jean-Philippe, Chen, Bin, Somayazulu, Maddury, Li, Jie, Ohtani, Eiji, Bass, Jay D.
Médium: Artigo
Jazyk:Inglês
Vydáno: National Academy of Sciences 2007
Témata:
Physical Sciences
On-line přístup:https://ncbi.nlm.nih.gov/pmc/articles/PMC1959425/
https://ncbi.nlm.nih.gov/pubmed/17686973
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.0706113104
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