Abstract:The study area is located in the south of Greater Khingan Range in Inner Mongolia Autonomous Region. It belongs to superposition part of the PaleoAsian metallogenic belt and the ircum Pacific metallogenic belt. Through geological survey of mineral resources, it is found that there are Fe, Cu and other multimetal mineralization in this area. According to analysis on rock characteristics, geophysical and geochemical anomalies and ore bodies characteristics, it is regarded that iron and copper deposit in this area is magma hydrothermal type with good metallogenic prospects. It will provide the basis for the further exploration of concealed ore deposits in this area.