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营房银铅锌矿是与重熔岩浆有关的浅成中低温热液裂隙充填型矿床。矿床主要受北北东向压扭断裂及沿断裂带隐爆—侵入角砾岩双重控制。本文在普查成果基础上,通过成矿地质背景、矿区地质概况和矿床地质特征的阐述,着重对矿床成因、成矿物质来源、找矿标志及成矿规律进行分析,认为该区具有较好的成矿地质条件和找矿前景,是寻找大中型银铅锌矿的有利地区。
Silver barite deposit in barrages is a type of epithermal fissure-filling mineralization associated with reclaimed magma. The deposit is mainly controlled by the north-north eastward compression buckling and the dual control of the implosion-brecciated breccia along the fault. Based on the results of the census, based on the geological background of mineralization, the geology of the mining area and the geologic characteristics of the deposit, the paper mainly analyzes the genesis of the deposit, the origin of the metallogenic material, the prospecting sign and the metallogenic regularity. Geological conditions of mineralization and prospects for prospecting, is to find a favorable area for large and medium-sized silver-zinc lead-zinc mine.