电邮这篇文章 Possible mantle phase transitions by the formation of SiO2 peroxides: Implications for mantle convection
- 作者: 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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隶属关系:
- Siberian Federal University
- Federal Research Center Krasnoyarsk Science Center, Siberian Branch
- Nikolaev Institute of Inorganic Chemistry, Siberian Branch
- 期: 卷 473, 编号 2 (2017)
- 页面: 416-418
- 栏目: Geology
- URL: https://ogarev-online.ru/1028-334X/article/view/189633
- DOI: https://doi.org/10.1134/S1028334X17040171
- ID: 189633
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详细
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.
作者简介
R. Khlebopros
Siberian Federal University; Federal Research Center Krasnoyarsk Science Center, Siberian Branch
编辑信件的主要联系方式.
Email: v.09@mail.ru
俄罗斯联邦, Krasnoyarsk, 640041; Krasnoyarsk, 660036
V. Zakhvataev
Siberian Federal University; Federal Research Center Krasnoyarsk Science Center, Siberian Branch
Email: v.09@mail.ru
俄罗斯联邦, Krasnoyarsk, 640041; Krasnoyarsk, 660036
S. Gabuda
Nikolaev Institute of Inorganic Chemistry, Siberian Branch
Email: v.09@mail.ru
俄罗斯联邦, pr. Akad Lavrentieva 3, Novosibirsk, 630090
S. Kozlova
Nikolaev Institute of Inorganic Chemistry, Siberian Branch
Email: v.09@mail.ru
俄罗斯联邦, pr. Akad Lavrentieva 3, Novosibirsk, 630090
V. Slepkov
Nikolaev Institute of Inorganic Chemistry, Siberian Branch
Email: v.09@mail.ru
俄罗斯联邦, pr. Akad Lavrentieva 3, Novosibirsk, 630090
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