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铅锌矿位于林东—乌兰浩特北东向岩浆构造带的西北侧,属于大兴安岭中段东南坡突泉—林西华力西、燕山期成矿带上。矿脉受北北西向压扭性构造裂隙控制,沿走向方向显舒缓波状。围岩蚀变与二迭系大石寨组的安山岩接触带形成10余米宽的硅化、绿泥石化、绿帘石化带,矿化体的成因为火山热液脉状。
The Pb-Zn deposit is located on the northwestern side of the NE-trending magmatic belt in the Rudong-Ulanhot, belonging to the Tuquan-Linxi Warisi-Yanshanian metallogenic belt on the southeast slope of the Greater Hinggan Mountains. The veins are controlled by the crushing of north-west and west-crushed tectonic fractures, and the veins are gently wavy along the strike direction. Surrounding rock alteration and Permian Dashizhai Formation andesite contact zone to form more than 10 meters wide silicification, chloritization, epidote petrochemical belt, mineralization of the genesis of volcanic hydrothermal veins.