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 Wulong-gou area are analyzed systematically from the perspective of strata,magmatic rocks and structures;finally,the metallogenic reg-ularity 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 ore-body 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 acti-vated 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.%五龙沟金矿是青海省东昆仑成矿带最具找矿潜力的矿床. 在搜集五龙沟地区金多金属矿床成矿大地构造背景、区域地层、岩性、构造、岩浆岩等方面资料的基础上,首先对区内典型金多金属矿床地质特征分别进行了描述,然后从地层、岩浆岩、构造等方面对区内金多金属矿床的控矿因素进行了系统分析,最后从矿床成矿时间、空间分布及成因等方面对成矿规律进行了总结. 结果表明:①五龙沟地区金多金属矿床产于构造韧性剪切带中,受构造及其演化控制明显;②金矿床在时间上具有多阶段性和长期性的分布规律,在空间上严格沿3条韧性、脆-韧性剪切带分布,各剪切带内矿床具有等距性和平行性的分布特点;③多金属矿床多分布于剪切带与后期NE—SW向的断裂带交汇部位,往往成群成组分布;④金矿体形成于多金属矿之前,以深部岩浆为主的壳幔混源、壳源是金多金属矿的重要成矿物质来源,伴随构造演化使成矿物质进一步活化并富集形成金多金属矿体. 上述研究成果对于区内进一步开展金多金属矿、构造热液蚀变型矿床的找矿工作具有一定的参考价值.
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