Отправить статью по E-mail Possible mantle phase transitions by the formation of SiO2 peroxides: Implications for mantle convection
- Авторы: 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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Учреждения:
- Siberian Federal University
- Federal Research Center Krasnoyarsk Science Center, Siberian Branch
- Nikolaev Institute of Inorganic Chemistry, Siberian Branch
- Выпуск: Том 473, № 2 (2017)
- Страницы: 416-418
- Раздел: Geology
- URL: https://ogarev-online.ru/1028-334X/article/view/189633
- DOI: https://doi.org/10.1134/S1028334X17040171
- ID: 189633
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Аннотация
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.
Об авторах
R. Khlebopros
Siberian Federal University; Federal Research Center Krasnoyarsk Science Center, Siberian Branch
Автор, ответственный за переписку.
Email: v.09@mail.ru
Россия, Krasnoyarsk, 640041; Krasnoyarsk, 660036
V. Zakhvataev
Siberian Federal University; Federal Research Center Krasnoyarsk Science Center, Siberian Branch
Email: v.09@mail.ru
Россия, Krasnoyarsk, 640041; Krasnoyarsk, 660036
S. Gabuda
Nikolaev Institute of Inorganic Chemistry, Siberian Branch
Email: v.09@mail.ru
Россия, pr. Akad Lavrentieva 3, Novosibirsk, 630090
S. Kozlova
Nikolaev Institute of Inorganic Chemistry, Siberian Branch
Email: v.09@mail.ru
Россия, pr. Akad Lavrentieva 3, Novosibirsk, 630090
V. Slepkov
Nikolaev Institute of Inorganic Chemistry, Siberian Branch
Email: v.09@mail.ru
Россия, pr. Akad Lavrentieva 3, Novosibirsk, 630090
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