Abstract
Using the method of thermodynamic simulation, the equilibrium composition of products of heating of plagioclases, pyroxenes, peridots, and magnetite is determined in a temperature range of 1000–1400°C in inert, oxidizing, and reducing atmospheres. The possibility of controlling the products of melting and crystallization of the above minerals is shown, and the behavior of a series of accessory metals (Ti, Mn, Cr, V) in these processes is evaluated.
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Original Russian Text © I.Z. Babievskaya, S.V. Fomichev, V.A. Krenev, 2009, published in Neorganicheskie Materialy, 2008, Vol. 45, No. 1, pp. 58–64.
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Babievskaya, I.Z., Fomichev, S.V. & Krenev, V.A. Equilibrium composition of products of melting of main minerals involved in the composition of basalt. Inorg Mater 45, 55–60 (2009). https://doi.org/10.1134/S0020168509010099
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DOI: https://doi.org/10.1134/S0020168509010099