河北兴隆水莲洞铜多金属矿矿化体特征及矿床成因探讨  

A Discussion on Characteristics of Copper and Mineral Deposits in Xinglong Wulian Cave,Hebei Province

作　　者：李智斌[1] 刘海波[1] 邢莞东 周海涛[1] LI Zhibin;LIU Haibo;XING Wandong;ZHOU Haitao(Eighth Geological Brigade of Hebei Geology and Mineral Resources Exploration Bureau, Qinhuangdao, Hebei 066001, China)

机构地区：[1]河北省地矿局第八地质大队,河北秦皇岛066001

出　　处：《中国锰业》2022年第2期55-60,共6页China Manganese Industry

基　　金：河北省地质矿产勘查开发局项目(454-0502-JBN-XXA9)。

摘　　要：河北水莲洞铜多金属矿位于河北省兴隆县蘑菇峪乡水莲洞村东山,处于马兰峪复式背斜中部北翼,矿区见有Cu、Pb、Zn、Mo、Ag、Au等矿化,作为马兰峪复背斜较典型的多金属矿床,研究总结其矿化特征、规律,对于马兰峪区域成矿规律总结、成矿体系建立具有较好的研究意义。Shuiliandong Copper Polymetallic Ore Deposit,located in Shuiliandong Village of Xinglong County of Hebei Province.It is in the north central wing of Malanyu compound anticline.There are mineralization of Cu,Pb,Zn,Mo,Ag and Au in the mining area.As a typical polymetallic deposit in malanyu complex anticline,it is of great significance to summarize the metallogenic regularities in establishing the metallogenic system in Malanyu region.

关 键 词：马兰峪复式背斜 铜多金属 矿化特征 矿床成因 

分 类 号：P618.2[天文地球—矿床学]