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Khlebopros, R. G.
Zakhvataev, V. E.
Slepkov, V. P.
Kuzmin, M. I.
2017-06-16T10:24:41Z
2017-06-16T10:24:41Z
2016-03
Khlebopros, R. G. On the possibility of phase transitions with the formation of SiO2 peroxide forms in the earth mantle and their effect on mantle convection [Текст] / R. G. Khlebopros, V. E. Zakhvataev, V. P. Slepkov, M. I. Kuzmin // Journal of Structural Chemistry. — 2016. — Т. 57 (№ 2). — С. 417-421
00224766
https://elib.sfu-kras.ru/handle/2311/32976
Текст статьи не публикуется в открытом доступе в соответствии с политикой журнала.
Based on the hypothesis advanced by S. P. Gabuda that the SiO2 molecule could undergo a transition from the linear form to the isomeric form with a ring-shaped (bent) structure, an idea is proposed that when the mantle substance melts, a phase transition of the bent SiO2 form into the linear SiO2 form can occur in the lower mantle. This phase transition might be of great importance for the lower-mantle convection processes and also for the rise of mantle plumes carrying both heat energy, and broad range of platinum group and rare elements to the Earth surface. © 2016, Pleiades Publishing, Ltd.
https://www.scopus.com/record/display.uri?eid=2-s2.0-84971642338&origin=resultslist&sort=plf-f&src=s&st1=Khlebopros&st2=&sid=AA3
mantle convection
peroxide forms
phase transitions
On the possibility of phase transitions with the formation of SiO2 peroxide forms in the earth mantle and their effect on mantle convection
Journal Article
Published Journal Article
417-421
37.31
2017-06-16T10:24:41Z
10.1134/S0022476616020256
Институт экологии и географии
Кафедра экологии и природопользования
Научно-исследовательская часть
Journal of Structural Chemistry
Q3
Q4


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