Normal>///The mother rock of Han-Xing type iron ore mineralization is the albitization and deironing magmatic rock. Its geological characteristics are evident, and forms close association of magnetite with magnetic anomaly and albitization. The scope, intensity, scale of albitization is positively related with the scale of magnetite. A comparison of the result can testifies the two results mutually and provides a basis for ore prospecting surrounding the existing orebodies so as to extend the scale and add more reserves at the bottom and the boundary of the existing ores, so a study on the genetic relation between albitization and metasomatic type iron deposit is of great significance for further prospecting in the region.