Northeastern Guangxi is tectonically located in the transition zone between the Jiangnan orogenic belt and the South China fold belt, and has a unique tectonic position. Using detailed analysis of a series of typical deposits and chronological data of granite related, along with deposit types and ore-forming elements, this paper divided the deposits in this area into six metallogenic systems. The formation of these deposits is closely related to tectonic-magmatic evolution in different periods and formed mainly at syn-collision compressional setting and/or post-collision extensional setting.