高密市菜园地区铅矿特征分析

Analysis of Lead Ore Characteristics in Caiyuan Area of Gaomi City

菜园铅矿床位于化山—王吴铅成矿带上,矿体受NE、NW向断裂控制,赋存于重晶石脉、石英脉及碎裂岩中。矿区圈定两个铅矿体,分别赋存于两条矿化蚀变带中。通过对菜园铅矿床地质条件、矿体的数量、空间分布、形态、矿床成因及找矿标志等进行具体阐述,为该区后续的找矿工作提供依据。

Caiyuan lead deposit is located in Huashan-Wangwu lead metallogenic belt.The ore body is controlled by NE and NW faults and occurs in barite veins,quartz veins and cataclastic rocks.Two lead ore bodies are delineated in the mining area and occur in two mineralized alteration zones respectively.The geological conditions of Caiyuan lead deposit,the quantity,spatial distribution,morphology,genesis and prospecting marks of the ore body are described in detail to provide basis for the subsequent prospecting work in this area.