广东梅县玉水铜多金属矿田矿床矿物学特征  

MINERALOGY OF THE YUSHUI Cu POLY-METALLIC DEPOSIT IN MEIXIAN, GUANGDONG

作　　者：郭锐 陈炳辉[2,2] 

机构地区：[1]广东有色地质勘查研究院,广州510080 [2]中山大学地质系,广州510275

出　　处：《矿产勘查》1999年第6期428-431,共4页Mineral Exploration

基　　金：国家教委博士点基金

摘　　要：着重研究梅县玉水铜多金属矿体中矿石的产出特征，黄铜矿、斑铜矿、辉铜矿、锌黝铜矿、锌砷黝铜矿、硫铜银矿、新发现的矿物硫铅铜矿（ 暂定名）The Yushui exceptionally rich copper deposit has been discovered in Meixian, Guangdong. The minerals include chalcopyrite, bornite, chalcocite, Zn-tetrahedrite, Zn-tennantite, stromeyerite and the new discovered Cu-Pb-S minerals. Its mineralogy and occurrence state of silver are studied.

关 键 词：矿物学特征 铜多金属矿床 玉水矿田 广东 

分 类 号：P618.41[天文地球—矿床学]