摘要
旺云山铜矿位于库米什—亦格尔达坂复式背斜中段转折端,彩花沟铜矿东延。矿化集中发育于下泥盆统阿尔彼什麦布拉克组中亚组第二岩性段,矿体主要赋存于富含硫化物的硅质岩,属(火山)喷流沉积型矿床。
Wangyunshan Copper Mine is located at the turning point of the middle part of Kumish-Yigeldaban anticline, and the Caihuagou Copper Mine extends eastward. Mineralization is concentrated in the second lithologic section of the Middle Asian Formation of the Albish Mabrak Formation of the Lower Devonian. The ore bodies are mainly hosted in sulfide-rich siliceous rocks and belong to (volcanic) exhalative sedimentary deposits.
作者
张永智
ZHANG Yong-zhi(Institute of Geology and Mineral Resources, Bureau of Non-ferrous Geological Exploration, Xinjiang Uygur Autonomous Region,Urumchi 830000,China)
出处
《世界有色金属》
2019年第1期107-107,110,共2页
World Nonferrous Metals
关键词
旺云山铜矿
喷流沉积型矿床
矿床成因
Wangyunshan copper deposit
jet sedimentary deposit
genesis of deposit
