Инд. авторы:	Bataleva Y.V., Palyanov Y.N., Sokol A.G., Borzdov Y.M., Bayukov OA
Заглавие:	The role of rocks saturated with metallic iron in the formation of ferric carbonate-silicate melts: experimental modeling under PT-conditions of lithospheric mantle
Библ. ссылка:	Bataleva Y.V., Palyanov Y.N., Sokol A.G., Borzdov Y.M., Bayukov OA The role of rocks saturated with metallic iron in the formation of ferric carbonate-silicate melts: experimental modeling under PT-conditions of lithospheric mantle // Russian Geology and Geophysics. - 2015. - Vol.56. - Iss. 1-2. - P.143-154. - ISSN 1068-7971. - EISSN 1878-030X.
Внешние системы:	DOI: 10.1016/j.rgg.2015.01.008; РИНЦ: 24019070; SCOPUS: 2-s2.0-84925300371; WoS: 000351312200008;
Реферат:	eng: Experimental modeling of the processes of formation of ferric carbonate-silicate melts through the carbonate-oxide-metal interaction is performed in the (Mg, Ca) CO3-SiO2-Al2O3-Fe-0 system at 6.3 and 7.5 GPa and within 1150-1650 degrees C, using a multianvil high-pressure apparatus of "split-sphere" type (BARS). Two parallel reactions run in the subsolidus region (1150-1450 degrees C): decarbonation, producing pyrope-almandine (Fe# = 0.40-0.75) and CO2 fluid, and redox interaction between carbonate and Fe-0, resulting in the crystallization of iron carbide in assemblage with magnesiowustite (Fe# = 0.75-0.85). It is shown that the reduction of carbonate or CO2 fluid by iron carbide and parallel redox interaction of magnesiowustite with CO2 produce graphite in assemblage with Fe3+-containing magnesiowustite. In the temperature range of 1450-1650 degrees C, generation of carbonate-silicate melts coexisting with pyrope-almandine, magnesiowustite, magnetite, ferrospinel, and graphite takes place. The composition of the produced melts is as follows: SiO2 approximate to 10-15 wt.%, S(FeO+ Fe2O3) = 36-43 wt.%, and Fe3+/Sigma Fe approximate to 0.18-0.23. These Fe3+-enriched carbonate-silicate melts/fluids are saturated with carbon and are the medium of graphite crystallization. Oxide and silicate phases (almandine, ferrospinel, and magnetite) coexisting with graphite are also characterized by high Fe3+/Sigma Fe values. It has been established that Fe3+-enriched carbonate-silicate melts can result from the interaction of Fe-0-containing rocks with carbonated rocks. In the reduced mantle (with the presence of iron carbides or oxides), melts of this composition can be the source of carbon and the medium of graphite crystallization at once. After separation and ascent, these ferric carbonate-silicate melts can favor oxidizing metasomatism in the lithospheric mantle. (C) 2015, V. S. Sobolev IGM, Siberian Branch of the RAS. Published by Elsevier B.V. All rights reserved.
Ключевые слова:	SYSTEMS; MOSSBAUER; OCEANIC-CRUST; NATURAL DIAMOND; MINERAL INCLUSIONS; EARTHS MANTLE; OXIDATION-STATE; DIAMOND FORMATION; CRYSTALLIZATION; high-pressure experiment; redox gradient; garnet; iron carbide; CO2 fluid; graphite; carbonate-silicate melt; OXYGEN FUGACITY;
Издано:	2015
Физ. характеристика:	с.143-154