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Experimental studies have been carried out to determine the phase equilibria for the ternary MgO-"FeO"-SiO2, in equilibrium with metallic iron. Liquiclus isotherms have been determined in the temperature range from 1 578 to 1 898K in the silica and pyroxene primary phase fields using high temperature equilibration, modified quenching and electron probe X-ray microanalysis (EPMA) techniques.

Phase Equilibria in the Cristobalite, Tridymite and Pyroxene Primary Phase Fields in the MgO-"FeO"-SiO2 System in Equilibrium with Metallic Iron