Zharigen iron deposit is located in the Sanjiang metallogenic belt Tuotuohe segment, which is located in the side of Qiangtang landmass between the lated Indo-Chinese epoch Bayanhar folding-orogenic belt and Qiangtang landmass the two major tectonic units. Ore body has been controlled by subvolcanic rocks and its internal early tectonic fissures, and genesis of this ore deposit belongs to subvolcanic magmatic hydrothermal type. However, the current mining area parts of 1∶2 000 magnetic anomaly are not checked or lack of deep drilling engineering project, and the depth control is not enough. It will be expanded resource perspective, if increase further verification efforts.