Инд. авторы:	Zhimulev E.I, Sonin V.M., Mironov A.M., Chepurov A.I.
Заглавие:	Effect of Sulfur Concentration on Diamond Crystallization in the Fe-C-S System at 5.3-5.5 GPa and 1300-1370 degrees C
Библ. ссылка:	Zhimulev E.I, Sonin V.M., Mironov A.M., Chepurov A.I. Effect of Sulfur Concentration on Diamond Crystallization in the Fe-C-S System at 5.3-5.5 GPa and 1300-1370 degrees C // Geochemistry International. - 2016. - Vol.54. - Iss. 5. - P.415-422. - ISSN 0016-7029. - EISSN 1531-8397.
Внешние системы:	DOI: 10.1134/S0016702916050116; РИНЦ: 27096516; SCOPUS: 2-s2.0-84971612055; WoS: 000376612300003;
Реферат:	eng: The paper presents results of experiments aimed at diamond synthesis in the Fe-C-S system at 5.3-5.5 GPa and temperatures of 1300-1370 degrees C and detailed data on the microtextures of the experimental samples and the composition of the accompanying phases (Fe3C and Fe7C3 carbides, graphite, and FeS). It is demonstrated that diamond can be synthesized after temperatures at which carbides are formed are overcome and can crystallize within the temperature range of 1300 degrees C (temperature of the peritectic reaction melt + diamond = Fe7C3) to 1370 degrees C (of thermodynamically stable graphite) under the appearance experimental pressure. The possible involvement of natural metal- and sulfur-bearing compounds in the origin of natural diamond is discussed.
Ключевые слова:	graphite; sulfides; iron carbides; GENESIS; GRAPHITE; MELTS; INCLUSIONS; AFRICAN DIAMONDS; PHYSICAL-PROPERTIES; YAKUTIAN KIMBERLITES; EARTHS MANTLE; SULFIDE-CARBON; high temperature; high pressure; NI-S; diamond;
Издано:	2016
Физ. характеристика:	с.415-422
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