Experimental phase equilibria studies have been carried out to investigate the phase chemistry in the CaO-"Fe 2 O 3 "-SiO 2 system related to the iron ore sinter making in 1 atm CO 2 at 1 200-1 230°C. The measurements have been performed using a modified experimental technique involving high temperature equilibration and rapid quenching followed by electron probe X-ray microanalysis (EPMA). In contrast to the equilibria in air, the experimental results show that no silico-ferrite of calcium (SFC solid solution) is formed in 1 atm CO 2 within the temperature range investigated; that is, the SFC phase is not stable at liquidus temperatures. The liquidus for the iron-rich corner of the CaO-"Fe 2 O 3 "-SiO 2 system in CO 2 atmosphere for the spinel (magnetite Fe 3 O 4) and dicalcium silicate (C 2 S = Ca 2 SiO 4) primary phase fields has been proposed.