近年来,会泽铅锌矿床在成矿物质来源、流体来源等方面取得了较大进展,同时前人对矿床成因进行了大量的研究(Zhou et al.,2001;韩润生等,2001),但这些模式均不能全面解释矿床的形成过程(黄智龙,2004)。本文在详细的野外调研基础上,以井下矿脉穿插关系为依据,对成矿阶段重新划分;同时,根据野外及室内矿相学观察,对矿石硫化物的产出形态、成分及形成先后关系进行厘定, In recent years, the Huize Pb-Zn deposit has made great progress in the source of ore-forming materials and the sources of fluids. In the meantime, a large number of studies have been conducted on the genesis of the deposit (Zhou et al., 2001; Han et al., 2001) All of these models can not fully explain the formation of the deposit (Huang Zhilong, 2004). On the basis of the detailed field investigation, this paper re-divided the metallogenic stage based on the interpenetration relationship of the underground veins. At the same time, according to the field and indoor mineralogical observations, the relationship between the output form, composition and formation of the sulfide ore Determined,