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作 者:李康东 郑忠超 罗平 黄鸿新 郑文斌 Li Kangdong;Zheng Zhongchao;Luoping;Huang Hongxin;Zheng Wenbin(Jiangxi Geology Bureau nuclear Geology brigade,shangrao,335000;Jiangxi Northeast Brigade of Jiangxi Bureau of Geology and Mineral Exploration and Development,Shangrao,334000)
机构地区:[1]江西省地质局核地质大队,上饶335000 [2]江西省地质局第八地质大队,上饶334000
出 处:《福建地质》2021年第4期299-305,共7页Geology of Fujian
基 金:江西省地质局科研项目“江西铜矿地质与勘查”的资助
摘 要:武夷山成矿带是我国重点成矿带之一,分布着众多的铜铅锌银等多金属矿床,矿床类型多样。通过对江西永平铜矿及其周边地质勘查工作,阐述了矿区地质特征、矿床特征,总结了矿床成因认识,探讨了找矿方向,并指出了矿区边深部的找矿思路。认为永平铜矿外围Ⅳ铜硫矿体可继续就矿找矿,且深部斑岩型钼矿还有很大找矿空间。Wuyishan metallogenic belt is one of the key metallogenic belts in China.There are many copper,lead,zinc and silver polymetallic deposits with various types in wuyishan metallogenic belt.Through the geological exploration of Jiangxi Yongping Copper Mine and its surrounding areas,we expounded the geological characteristics,the deposit characteristics,summarized the formation understanding of the deposit,discussed the prospecting direction,and pointed out the deep prospecting idea of the mining area.It is believed that the NO.Ⅳcopper-sulfur body outside Yongping copper mine can continue to mine,and there is still a lot of prospecting space for deep porphyry molybdenum mine.
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