CAJ | 학술논문

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。
오가루동광위중저온열액맥형동광상。통과보사대오가루동광상적지질특정、공광인소급광상성인적계통연구，인위광구NW향단렬공제료함동석영맥급공작석화중정석화쇄렬암적분포。재분석조광표지적기출상，응진일보개전지구물이화학감사，가대광구심부급외위적조광력도，이기발현신적동광체。
Wujialou copper deposit is a medium low 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 copper bearing 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.