The corundum in Fuping area of Hebei Province was taken as the studied object to probe into the occurrence characteristics and genesis of migmatite corundum. The mineral paragenetic association, texture and paragenetic sequence of minerals of corundum were investigated by means of mineralogy, petrology and geochemistry, and the formation mechanism of corundum in this area was discussed. The size of the corundum is generally large, and the associated minerals are mainly K-feldspar, plagioclase, biotite, muscovite, sillimanite, rutile, chlorite, magnetite, ilmenite, and apatite. According to petrographic characteristics, it is inferred that the corundum was formed by crystallization of aluminum-rich magma in the process of migmatization. The gemological significance of the migmatite corundum was studied, and the result shows that the migmatite corundum can reach the gem grade, although it is difficult for this mineral to achieve the fine grade. The large-scale development and utilization of this mineral should implement targeted improvement and treatment.