茶尖岭矿区后水矿化点铜银多金属成矿条件分析及远景初探  

Metallogeny of Copper and Siver Polymetallic Ore Deposits at Houshui Mineralization Spot in Chajianling Mine and Its Outlook for Prospecting

作　　者：曹希英 高原冰 王高峰[1] 张永力[1] 

机构地区：[1]吉林省有色金属地质勘查局607队,吉林吉林132013

出　　处：《矿产与地质》2012年第1期45-51,共7页Mineral Resources and Geology

摘　　要：茶尖岭矿区后水矿化点铜银多金属矿属于浅成热液脉型成因,通过矿床形成的热源、水源、矿源的信息标志分析了后水矿化点铜银多金属成矿条件。认为该矿化点铜银多金属成矿的热源、水源、矿源条件均较充足,指出找矿有利地段。The copper and silver polymetallic ore deposits at Houshui mineralization spot in Chajianling ore field belong to epithermal vein type deposit. The metallogenic conditions of copper and silver polymetallic de- posit were analyzed based on the indicators of hot source, water source and ore matter source information for mineralization. It is believed that the conditions of hot source, water source and ore matter for the formation of copper and silver polymetallic ores is sufficient and several favorable locations for ore prospecting was sug- gested in the paper.

关 键 词：铜银多金属矿床 浅成热液脉型成因 三源汇聚区 找矿远景区 

分 类 号：P618.52[天文地球—矿床学]