摘要
哈密铜山矿区位于博格达-哈尔雷克晚古生代岛弧东段,处于准噶尔古板块北天山弧盆带,是新疆重要的金属成矿区之一。文章结合区域成矿地质背景,通过对矿区地质特征、铜多金属矿体特征分析,总结了矿床成因。
Hami tongshan mining area is located in bogurda-Hal lake in east section of late Paleozoic island arc,junggar old plates in the north tianshan arc basin,is one of important metal metallogenic province of xinjiang.Combining with regional ore-forming geological background,geological characteristics,the mining area through analysis of characteristics of copper polymetallic ore body,ore deposit formation are summarized.
出处
《世界有色金属》
2017年第3期221-221,223,共2页
World Nonferrous Metals
关键词
新疆哈密
铜多金属矿床
铜山
地质特征
矿床成因
Xinjiang hami
Copper polymetallic deposit
Quotation
Geological characteristics
Genesis
