摘要
The ore body exists in the marble, which is near the fault and over the granite. The contact between marble and granite is the main metallogenetic part. There is a thick metallogenetic bed of intense ferritization and weak Pb-Zn metallogenesis at Dakuangshan, Xiaoshilin and Huiyao, etc. According to the exploration, the authors believe that this orefield has the prospects of finding out a middle-large scale ore deposit.