Abstract:The Denggezhuang gold deposit lies in the Muping-Rushan gold mineralization belt, eastern Shandong Province. The exposed strata in the ore district are dominated by Archean Jiaodong Group and Proterozoic Jingshan Group, where well-developed faults control most of the ore veins striking in NE and NNE directions. The secondary faults which control ores formed in the same time as the Jinniushan fault. Analysis of the relationship between fault structure and gold mineralization suggests that this deposit can be divided into structural systems of pre-mineralization, co-mineralization and postmineralization. The principal compressive stress of the co-mineralization time is in NNW-SSE direction. And the stress field of this deposit might have experienced an evolution from nearly SN compression to NNW-SSE compression and to NWW-SEE compression.