摘要
对长江中下游（包括赣北地区）主要的铜矿床成因类型进行了阐述，并对层状铜矿床的成因进行分析，提出了找矿方向。
The main genetic type of copper deposits are discribed in medium and downstream ofChangjiang River(included the north of Jiangxi Province), and the genesis of the bedded copperdeposits have been analysed. At the same time, the prospects of the bedded copper deposits arepointed out.
出处
《有色矿山》
2000年第1期1-5,共5页
Nonferrous Mines
关键词
铜矿床
基本特征
成因浅析
层状铜矿
bedded copper deposit
basic character
submarine eruptive sedimentation
