福建顺昌黄梓厂铜多金属矿地质特征及找矿前景分析  

On the Geological Characteristics and Ore-finding Perspective of Huangzichang Copper Polymetallic Deposit in Shunchang County,Fujian Province

作　　者：王协胜 

机构地区：[1]福建省闽北地质大队,福州350002

出　　处：《福建地质》2014年第1期8-14,共7页Geology of Fujian

基　　金：2004年国家资源补偿费项目-福建省顺昌县黄梓厂矿区铜铅锌矿普查

摘　　要：顺昌黄梓厂铜多金属矿床位于闽西北隆起带与闽西南坳陷带接合部的北侧,矿体呈层状、透镜状贮存于焦坑组北西向、北北西向层间破碎带中。成矿物质来自含矿地层及后期岩浆热液,属中低温热液充填型矿床。Huangzichang copper polymetallic deposit in Shunchang county is situated at the uplift belt of the northwestern Fujian and the north of depression belt ioints of the southwestern Fujian. The orebodys in a quasi-layer and lenticular are stored in Jiaokeng Group NW and NNW trending interlayer fracture zone. Ore-forming meterials come from the ore-berating formation and late magmatic hydrothermal. It belongs to the medium-low temperated filling- type deposit.

关 键 词：铜多金属矿 地质特征 找矿前景 顺昌黄梓厂 

分 类 号：P618.2[天文地球—矿床学]