Zobrazeno 1 - 8
of 8
pro vyhledávání: '"D. M. Soultanov"'
Publikováno v:
Geology of Ore Deposits. 65:56-71
Autor:
N. S. Gorbachev, A. N. Nekrasov, D. M. Soultanov, P. N. Gorbachev, A. V. Kostyuk, Yu. B. Shapovalov
Publikováno v:
Doklady Earth Sciences. 497:206-210
The liquid phases are represented by immiscible Fe–S and Fe–C melts under partial melting of the graphite-saturated Fe–S–C system at P = 0.5 GPa and T = 1150, 1200, and 1250°C. Fe, Ni, Pt, and Au are predominantly concentrated in the Fe–C
Publikováno v:
Петрология. 27:606-616
To obtain new data on the phase relationships in the fluid-containing upper mantle at P up to 4 GPa, T up to 1400C, partial melting of H2O-containing peridotite, basalt, as well as peridotite-basalt association with an alkaline-carbonate fluid was ex
Autor:
Yu. B. Shapovalov, D. M. Soultanov, N. S. Gorbachev, A. N. Nekrasov, P. N. Gorbachev, A. V. Kostyuk
Publikováno v:
Доклады Академии наук. 489:393-398
The phase relationships have been experimentally studied at eclogitization of basalts and the melting of H2O‑containing eclogite in the basalt-H2O system at P = 3,7-4,0 GPa, T = 1000-1300 °C. It is established that the phase relationships depend o
Autor:
A. N. Nekrasov, D. M. Soultanov, N. S. Gorbachev, Yu. B. Shapovalov, P. N. Gorbachev, A. V. Kostyuk
Publikováno v:
Doklady Earth Sciences. 489:1421-1425
The phase relations upon eclogitization of basalt and melting of H2O-bearing eclogite were studied experimentally for basalt–H2O in the range of P = 3.7–4.0 GPa and Т = 1000–1300°C. It is shown that the phase relations depend on temperature.
Autor:
D. M. Soultanov, P. N. Gorbachev, A. V. Kostyuk, A. N. Nekrasov, N. S. Gorbachev, Yu. B. Shapovalov
Publikováno v:
Доклады Академии наук. 488:640-644
The phase relations in the phlogopite-carbonate system were studied at P = 3.8 GPa, T = 1200-1300 C. The interaction of phlogopite with carbonate melt resulted in the formation of a polymineral association of relic and newly formed phases of the phlo
Autor:
Yu. B. Shapovalov, D. M. Soultanov, N. S. Gorbachev, A. N. Nekrasov, P. N. Gorbachev, A. V. Kostyuk
Publikováno v:
Doklady Earth Sciences. 488:1240-1244
Phase relations in the phlogopite–carbonate system were studied at P = 3.8 GPa and T = 1200–1300°C. The interaction of phlogopite with the carbonate melt resulted in the formation of a polymineral association of relict and newly formed phases of
Publikováno v:
Advances in Experimental and Genetic Mineralogy ISBN: 9783030428587
The article presents the results of experiments at pressure 4.0 GPa and temperature 1400 °C on the influence of fluids (H2O, H2O + CO2, H2O + HCl) on the composition of restite and magma formed during the melting of the peridotite-basalt-(K, Na)2CO3
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1cc91af6426ad39c6d954d08bf846479
https://doi.org/10.1007/978-3-030-42859-4_12
https://doi.org/10.1007/978-3-030-42859-4_12