Enviar artigo por via de e-mail Possible mantle phase transitions by the formation of SiO2 peroxides: Implications for mantle convection
- Autores: Khlebopros R.G.1,2, Zakhvataev V.E.1,2, Gabuda S.P.3, Kozlova S.G.3, Slepkov V.A.3
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Afiliações:
- Siberian Federal University
- Federal Research Center Krasnoyarsk Science Center, Siberian Branch
- Nikolaev Institute of Inorganic Chemistry, Siberian Branch
- Edição: Volume 473, Nº 2 (2017)
- Páginas: 416-418
- Seção: Geology
- URL: https://ogarev-online.ru/1028-334X/article/view/189633
- DOI: https://doi.org/10.1134/S1028334X17040171
- ID: 189633
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Resumo
On the basis of quantum–chemical calculations of the linear to isomeric bent transition of the SiO2 molecule, it is suggested that the bent to linear transition of SiO2 forms can occur in melted mantle minerals of the lower mantle. This may be important for the formation of the peculiarities of mantle convection and origination of plumes.
Sobre autores
R. Khlebopros
Siberian Federal University; Federal Research Center Krasnoyarsk Science Center, Siberian Branch
Autor responsável pela correspondência
Email: v.09@mail.ru
Rússia, Krasnoyarsk, 640041; Krasnoyarsk, 660036
V. Zakhvataev
Siberian Federal University; Federal Research Center Krasnoyarsk Science Center, Siberian Branch
Email: v.09@mail.ru
Rússia, Krasnoyarsk, 640041; Krasnoyarsk, 660036
S. Gabuda
Nikolaev Institute of Inorganic Chemistry, Siberian Branch
Email: v.09@mail.ru
Rússia, pr. Akad Lavrentieva 3, Novosibirsk, 630090
S. Kozlova
Nikolaev Institute of Inorganic Chemistry, Siberian Branch
Email: v.09@mail.ru
Rússia, pr. Akad Lavrentieva 3, Novosibirsk, 630090
V. Slepkov
Nikolaev Institute of Inorganic Chemistry, Siberian Branch
Email: v.09@mail.ru
Rússia, pr. Akad Lavrentieva 3, Novosibirsk, 630090
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