对大溶溪白钨矿床成矿地质特征和富集条件进行了分析 ,并指出成矿作用是在含钨建造钨初始富集的基础上 ,在花岗岩侵入产生的巨大热力驱动下发生的。特定层位和岩体是其成矿的必要条件 ,属似矽卡岩型白钨矿床。矿区与外围以及岩体周边具有发现同类型白钨矿床的前景。 The metallogenic geological characteristics and enrichment conditions of the Daciuxi scheelite deposit are analyzed. It is pointed out that the mineralization occurred under the great thermal power generated by granite intrusion on the basis of initial tungsten enrichment of tungsten. Specific horizon and rock mass are the necessary conditions for its metallogenesis, similar to the skarn type scheelite deposit. Prospects for the discovery of the same type of scheelite deposits are located in the mine area and its perimeter and in the vicinity of the rock mass.