长江中下游地区层状铜矿床基本特征及成因  

GENESIS AND BASIC CHARACTERISTICS OF LAYERED COPPER ORE DEPOSIT IN MIDDLE lOWER REACHES OF YANGZI RIVER

作　　者：唐俊华[1] 

机构地区：[1]江西铜业公司武山铜矿,江西瑞昌332204

出　　处：《矿产与地质》2000年第2期76-80,共5页Mineral Resources and Geology

摘　　要：阐述了长江中下游 (包括赣北地区 )主要的铜矿成因类型暨沉积—海底喷流沉积层状铜 (S,Au,Ag)矿床 ,并对层状铜矿床的成因进行分析 。In this paper the main genesis types of copper ore deposits and deposit layered copper (including S,Au,Ag) ore deposits formed by spouting in ocean bottom have been introduced.The genesises of the layered coppor ore deposits have been studied,and the direction of searching for the kind of ore deposits have been pointed out.

关 键 词：层状铜矿床 基本特征 海底喷流沉积 矿床成因 

分 类 号：P618.410.2[天文地球—矿床学] P618.410.1[天文地球—地质学]