Abstract: Wulonggou gold deposit is the most potential mineralization deposit in eastern Kunlun metallogenic belt of Qinghai province.Based on collecting the geological information of Wulonggou gold deposit including its ore-forming tectonic background，regional strata and intrusions，structure and so on，firstly，the geological characteristics of typical gold-polymetallic deposits in Wulonggou area are analyzed in depth；then，the ore-controlling factors of the gold-polymetallic deposits in Wulonggou area are analyzed systematically from the perspective of strata，magmatic rocks and structures；finally，the metallogenic regularity of the gold-polymetallic in Wulonggou area are summarized from the aspects of metallogenic time，space distribution and ore genesis.The results show that：①Wulonggou gold deposit is located in the ductile shear zones and it is controlled obviously by the structure evolution；②the gold deposits have the multiple stages and long-term distribution regularities in time domain while in spatial domain，the gold deposits are along the three ductile and brittle-ductile shear zones strictly，the deposits within the shear zones has the distribution characteristics of equidistance and parallelism；③the gold-polymetallic deposits are located in the intersection zones of the shear zones and NE-SW trending fault，they are distributed in groups frequently；④the gold orebody is formed before the polymetallic ore，deep magma is the main composition of crust-mantle mixed source and crust source，they are the important source of ore-forming materials，associated with the tectonic evolution，the ore-forming materials are activated further and enriched into polymetallic orebody.The above research results have some reference for the further prospecting work of gold-polymetallic and tectonic hydrothermal alteration type deposits in this area.

Key words: Gold-polymetallic, Geological characteristics of deposits, Ore-controlling factors, Genesis of mineral deposit, Mineralization regularity, Prospecting work