Abstract：In order to explore the process mineralogy characteristics of Baima vanadium-titanium magnetite from Panxi area, some advanced analysis methods including chemical analysis, optical microscope (OM), scanning electron microscope (SEM), automated mineral identification and characterization system (AMICS) were employed to deeply study the ore of Baima vanadium-titanium magnetite. The results showed that the main minerals of ore included titanomagnetite, ilmenite, anorthite, diopside and serpentine. The mass fraction of Fe, Ti and V in ore was 25.05%, 3.46% and 0.13%, respectively. These elements could be comprehensively recycled and utilized. The proportion of iron in the form of titanomagnetite was 74.13%, while 13.16% of iron existed in the form of iron-containing silicate. 63.72% of titanium existed in the form of independent ilmenite mineral and ilmenite (chadacryst), and 33.67% of titanium existed in titanomagnetite in the form of isomorphism. The titanomagnetite, ilmenite and sulfur minerals mainly existed in medium grains, while the disseminated grain size of most ilmenite (chadacryst) and magnesium aluminate spinel (chadacryst) was particle (less than 0.010 mm). 13.16% of iron in ore existed in silicate as well as titanium-containing iron ore (chadacryst) and magnesium aluminate spinel (chadacryst) in most titanomagnetite, which was the main factor influencing the grade of iron concentrate.
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