摘要
Dicili Pb-Zn deposit is in Pantiange fault and Guazhuagua fault.In this area,the sedimentation,magmatism and metamorphism are controlled strictly by 2 faults.The regional metallogenetic geological conditions are very advantageous.We preliminarily think it belongs to the mid-low T hydrothermal Pb-Zn deposit controlled by structural fracture-fissure zone and strata together in genesis.