山东诸城吴家楼铜矿床地质特征及找矿前景

Geological Characteristics and Prospecting Potentiality of Wujialou Copper Deposit in Zhucheng City of Shandong Province

摘要:

吴家楼铜矿为中低温热液脉型铜矿床。通过普查对吴家楼铜矿床的地质特征、控矿因素及矿床成因的系统研究，认为矿区NW向断裂控制了含铜石英脉及孔雀石化重晶石化碎裂岩的分布。在分析找矿标志的基础上，应进一步开展地球物理化学勘查，加大矿区深部及外围的找矿力度，以期发现新的铜矿体。

Abstract:

Wujialou copper deposit is a mediumlow temperature hydrothermal type copper deposit. Based on the study of geological characteristics, controlling factors, origin of Wujialou copper deposit, it is regarded that faults with the trend of NW have controlled the driection of copperbearing quartz vein and malachitization, baratization cataclasite. On the basic of analyzing prospecting criterias, it is supposed to increase much more efforts in deep and peripheral prospecting in a view to discover new copper bodies.