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凤凰山Ag－Pb-Zn多金属矿床产在寒武系类复理石建造中，赋矿围岩为砂岩和页岩，矿体受北西西向的构造破碎带控制。含矿热液流体沿构造破碎带充填，形成规模较大的多金属矿床，矿床的形成具有多期多阶段的特征。银主要以银的独立矿物形式存在，和方铝矿、硫锰矿、闪锌矿、菱锰矿及黄铁矿的关系较为密切。主要的银矿物有辉锑铅银矿、深红银矿、杂辉锑银铅矿、捷辉锑银铅矿、柱硫锑铅银矿、脆银矿、辉锑银矿和银黝铜矿等。银矿物主要形成于石英-硫化物阶段和石英-碳酸盐、硫盐阶段。
The Fenghuangshan Ag-Pb-Zn polymetallic deposit is produced in the Cambrian-type flysch. The ore-bearing rocks are sandstone and shale, and the orebodies are controlled by the NW-trending structural crust. The ore-bearing hydrothermal fluids fill the structural crustal zone to form a large-scale polymetallic ore deposit. The formation of the ore deposit has the characteristics of multi-stage and multi-stage. Silver is mainly in the form of silver as an independent mineral, which is closely related to feldspar, manganese ore, sphalerite, rhodochrosite and pyrite. The main silver minerals are Hui-antimony lead-silver mine, deep red silver mine, antimony antimony silver lead mine, Jie Hui antimony silver lead ore, lead antimony lead silver mine, brittle silver mine, stibnite mine and silver tetrahedrite Wait. Silver minerals are mainly formed in the quartz-sulphide and quartz-carbonate and sulfur phases.