Zobrazeno 1 - 9
of 9
pro vyhledávání: '"V. M. Ryzhkov"'
Publikováno v:
Литосфера, Vol 20, Iss 5, Pp 682-689 (2020)
Research subject. The Karabash ore district is a unique structural zone in the Ural folded system, formed at the joint of the Magnitogorsk and Tagil depressions. The uniqueness of this zone is associated with its specific formation conditions: a Pale
Externí odkaz:
https://doaj.org/article/e542a2f8c6364363b2bf9eec1b4226a3
Publikováno v:
Литосфера, Vol 18, Iss 5A, Pp 48-56 (2020)
The determination of ancient ages of zircons in dunites from the orogenic regions and central-type platform massifs raised a number of issues: 1) the equilibrium of zircon with dunite material and, as a result, the possibility of determining the age
Externí odkaz:
https://doaj.org/article/2b06e5468a754e05bdc45c3998c5a380
Autor:
M. A. Igumentseva, L. Y. Kabanova, V. N. Anfilogov, M. V. Shtenberg, I. A. Blinov, V. M. Ryzhkov
Publikováno v:
Литосфера, Vol 19, Iss 4, Pp 588-597 (2019)
Research subject. In this research, we studied lenses, nodules and interlayers of granulated quartz, which are located in amphibolites and shales in the eastern part of the Ufalei gneso-amphibolite complex.Materials and methods. Petrographic features
Externí odkaz:
https://doaj.org/article/f59bf0ab33344fe1813826f71e6d2c9c
Publikováno v:
Doklady Chemistry. 504:122-125
Publikováno v:
Doklady Earth Sciences. 469:824-827
The results of study of phase equilibria in the MgO–SiO2–ZrO2 system at 1450–1550°C are reported. The studied system contains two eutectic points and six fields: (I) MgSiO3 + SiO2; (II) MgSiO3 + ZrO2; (III) ZrSiO4 + SiO2; (IV) MgSiO3 + Mg2SiO4
Publikováno v:
Inorganic Materials. 52:655-660
We report a process for the preparation of ultrafine silicon carbide powder in a self-contained protective atmosphere. The protective atmosphere is ensured by the silicon monoxide released during the carbothermal synthesis. A reactor design is propos
Publikováno v:
Doklady Earth Sciences. 475:946-948
The problem of the U–Pb age of zircon crystals from ultrabasic rocks is discussed in this paper. It is shown that the assumption on the xenogenic nature of zircon crystals in dunite is not consistent with the petrographic and experimental data. The
Autor:
L. Ya. Kabanova, V. M. Ryzhkov, I. A. Blinov, P. M. Valizer, A. A. Krasnobaev, V. N. Anfilogov
Publikováno v:
Doklady Earth Sciences. 464:963-966
The results of experimental studies of interaction between zircon crystals and dunite at 1400–1550°C are given. At 1400°C no interaction of zircon with dunite takes place. At higher temperatures zircon interacts with olivine forming eutectoid mix
Publikováno v:
Doklady Chemistry. 460:10-12