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顺元昌铅锌矿位于内蒙大兴安岭多金属成矿带内,矿体围岩为林西炭质板岩及粉砂质板岩,成矿与燕山早期花岗岩体相关。区内矿体在时空分布上具有规律性,在空间上有分带现象,在时间上有分期的特点,矿床形成划分为两个成矿期次,由于各期次的成矿作用不同,分别形成矽卡岩型矿床和斑岩型矿床。其中矽卡岩型矿床与燕山早期花岗岩关。
The Shunchang Pb-Zn deposit is located in the Daxinganling polymetallic metallogenic belt in Inner Mongolia. Its ore body is Linxi carbonaceous slate and silty slate, and its mineralization is related to the early Yanshan granite. The ore bodies in the area have regularity in space-time distribution, with zonation in space and staging in time. The ore deposits are divided into two metallogenic stages. Because of the different mineralization stages, Formation of skarn deposits and porphyry deposits. Among them, skarn-type deposits are related to early Yanshan granite.