“…Zhang et al [39] investigated martensitic FeeNi alloys aged in the 300e450 C temperature range and measured a-Fe and g-(Fe, Ni) FM phase compositions in this range. They did not find experimental evidence of the monotectoid equilibrium at temperature lower than 400 C. Combining the results of previous investigations [28,30,31,39] with new measurements on meteoric samples Yang, Williams and Goldstein [12] concluded that the monotectoid equilibrium should occur at about 400 C with phase compositions of about 6 [28], 40 and 46 at% Ni [39] for a-Fe, g-(Fe,Ni) PM and g-(Fe, Ni) FM , respectively.…”