Zobrazeno 1 - 10
of 27
pro vyhledávání: '"N. I. Suk"'
Autor:
B. B. Damdinov, A. R. Kotelnikov, N. I. Suk, L. B. Damdinova, Z. A. Kotelnikova, G. M. Akhmedzhanova, Y. B. Shapovalov
Publikováno v:
Doklady Earth Sciences. 507:1026-1032
Publikováno v:
Geology of Ore Deposits. 64:104-122
Publikováno v:
Petrology. 29:561-574
Data on Na and K distribution between feldspar and solution at 550°C and 1.5 kbar under hydrothermal conditions were obtained in experiments on cation-exchange equilibria of gallium feldspars according to the reaction NaGaSi3O8 + KCl aq = KGaSi3O8 +
Publikováno v:
Doklady Earth Sciences. 498:477-481
The solubility of phenakite in aluminosilicate melts of various alkalinity was studied experimentally at T = 1000°C and P = 1 kbar in dry conditions and in the presence of 10 wt % H2O. The experiments were carried out on a high gas pressure vessel.
Autor:
I. S. Peretyazhko, A. R. Kotelnikov, A. N. Sapozhnikov, N. I. Suk, E. A. Savina, R. Y. Shendrik
Publikováno v:
Petrology. 28:221-245
The paper reports the results of melting experiments on the fluorite-enriched rhyolites of the Nyalga Basin (Central Mongolia). The fluoride–calcium (F–Ca) melt was obtained in a wide range of P-T parameters (1250–750°С, 5.5–1 kbar). Fluori
Autor:
K. V. Martynov, A. R. Kotelnikov, N. I. Suk, O. T. Gavlina, G. M. Akhmedzhanova, V. A. Suvorova
Publikováno v:
Геохимия. 64:1047-1063
For the development of methods for the disposal of radioactive waste in the rocks of the earths crust, the concept of phase and chemical correspondence in the system of matrix material ― host rock has been proposed. This principle allows directiona
Autor:
O. T. Gavlina, K. V. Martynov, V. A. Suvorova, N. I. Suk, A. R. Kotelnikov, G. M. Akhmedzhanova
Publikováno v:
Geochemistry International. 57:1066-1081
A concept of phase and chemical correspondence in the system matrix material–host rock is suggested for methods of storing radioactive wastes in crustal rocks. This principle allows directional synthesis of certain mineral matrixes. Matrix material
Publikováno v:
Petrology. 27:534-551
The paper reports the results of an experimental study of phase relations and distribution of elements in silicate melt–salt melt systems (carbonate, phosphate, fluoride, chloride), silicate melt I – silicate melt II, and fluid–magmatic systems
Publikováno v:
Доклады Академии наук. 484:595-599
The melting in the system of aluminosilicate (granite) melt — fluoride salt melt at T = 800–1200˚C and P = 1–2 kbar was experimentally investigated. The data on the phase composition of silicate-salt systems and the character of the interphase
Publikováno v:
Petrology. 27:186-201
Liquid immiscibility was studied in melting experiments in the system trachyrhyolite–water + salt (NaF, Na2CO3) conducted at parameters imitating those of the volcanic process. The indicator components were La, Nb, Sr, W, Mo, Cr, Fe, Rb, and Cs. Th