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结合成矿区域地质背景,在研究铅锌矿的矿体特征、矿物组分、矿石结构构造及矿物共生组合的基础上,对矿床成因进行了分析,认为区内铅锌矿床为浅成低温热液型铅锌矿床,其形成经历了构造热液成矿期及后生氧化富集阶段。对找矿标志做了深层次探讨,总结了石寨坪铅锌矿找矿标志,这对该区域的铅锌矿勘查、研究有着重要的理论指导意义。
Based on the geological background of the metallogenic region, the genesis of the deposit is analyzed on the basis of the research on the ore body characteristics, mineralogical composition, ore structure and mineral assemblage of lead-zinc deposits. It is considered that the lead-zinc deposits in the area are shallow to low temperature The liquid-type lead-zinc deposits have undergone tectono-hydrothermal mineralization and epigenetic enrichment. Depth exploration of prospecting signs and summarizes the prospecting marks for the Shizhaoping lead-zinc mine, which has important theoretical guidance for the exploration and study of lead-zinc deposits in the region.