Инд. авторы:	Bataleva Y.V., Palyanov Y.N., Borzdov Y.M., Bayukov O.A., Sobolev N.V.
Заглавие:	Conditions for diamond and graphite formation from iron carbide at the P-T parameters of lithospheric mantle
Библ. ссылка:	Bataleva Y.V., Palyanov Y.N., Borzdov Y.M., Bayukov O.A., Sobolev N.V. Conditions for diamond and graphite formation from iron carbide at the P-T parameters of lithospheric mantle // Russian Geology and Geophysics. - 2016. - Vol.57. - Iss. 1. - P.176-189. - ISSN 1068-7971. - EISSN 1878-030X.
Внешние системы:	DOI: 10.1016/j.rgg.2016.01.012; РИНЦ: 26856026; SCOPUS: 2-s2.0-84958609299; WoS: 000369723900013;
Реферат:	eng: To estimate conditions for the stability of iron carbide under oxidation conditions and to assess the possibility of formation of elemental carbon by interaction between iron carbide and oxides, experimental modeling of redox interaction in the systems Fe3C-Fe2O3 and Fe3C-Fe2O3-MgO-SiO2 was carried out on a split-sphere high-pressure multianvil apparatus at 6.3 GPa and 900-1600 degrees C for 18-20 h. During carbide-oxide interaction in the system Fe3C-Fe2O3, graphite crystallizes in assemblage with Fe3+-containing wusite. Graphite forms from carbide carbon mainly by cohenite oxidation: Fe3C + 3Fe(2)O(3) -> 9FeO + C-0 and FeO + Fe3C -> (Fe2+, Fe3+)O + C-0. At above-solidus temperatures (>= 1400 degrees C), when metal-carbon melt is oxidized by wusite, graphite and diamond crystallize by the redox mechanism and form the Fe3+-containing wstite + graphite/diamond assemblage. Interaction in the system Fe3C-Fe2O3-MgO-SiO2 results in the formation of Fe3+-containing mannesiowusite-olivine-graphite assemblage. At >= 1500 degrees C, two melts with contrasting f(O2) values are generated: metal-carbon and silicate-oxide; their redox interaction leads to graphite crystallization and diamond growth. Under oxidation conditions, iron carbide is unstable in the presence of iron, silicon, and magnesium oxides, even at low temperatures. Iron carbide-oxide interaction at the mantle temperatures and pressures leads to the formation of elemental carbon; graphite is produced from carbide carbon mainly by redox reactions of cohenite (or metal-carbon melt) with Fe2O3 and FeO as well as by interaction between metal-carbon and silicate-oxide melts. The results obtained suggest that cohenite can be a potential source of carbon during graphite (diamond) formation in the lithospheric mantle and the interaction of iron carbide with iron, silicon, and magnesium oxides, during which carbon is extracted can be regarded as a process of the global carbon cycle. (C) 2016, V.S. Sobolev IGM, Siberian Branch of the RAS. Published by Elsevier B.V. All rights reserved.
Ключевые слова:	MOSSBAUER; FERRIC IRON; REDOX BUDGET; SUBDUCTION ZONES; KOKCHETAV MASSIF; HIGH-PRESSURE; MINERAL INCLUSIONS; EARTHS MANTLE; DEEP CARBON-CYCLE; lithospheric mantle; redox interaction; subduction; olivine; oxides; diamond; graphite; wusite; iron carbide; high-pressure experiment; METAL;
Издано:	2016
Физ. характеристика:	с.176-189
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