摘要
盼水河锑矿床位于新疆维吾尔自治区。矿区内赋矿地层为中二叠世黄羊岭群浅海-深海相浊积岩建造。区内构造发育,沿断裂带岩石破碎、硅化普遍,次生石英岩脉发育。矿床受断裂构造控制明显,矿床成因属岩浆期后低温热液充填型矿床。
The Xinshui River antimony deposit is located in Xinjiang Uygur Autonomous Region.The ore bearing strata in the mining area are the shallow marine deep-sea turbidite formation of the Middle Permian Huang Yang Ling group.The development of tectonic magmatic rocks in the area is generally broken and silicified along the fault zone,and secondary quartz veins are developed.The deposit is controlled obviously by the fault structure.The deposit belongs to the post magmatic hypothermal hydrothermal filling type deposit.
作者
刘亚明
LIU Ya-ming(Hebei geology and Mineral Bureau Sixth Geological Brigade,Shijiazhuang 050081,China)
出处
《世界有色金属》
2018年第10期167-167,169,共2页
World Nonferrous Metals
关键词
盼水河锑矿
中二叠世黄羊岭群
构造-岩浆岩
低温热液矿床
the Pan Shui River antimony deposit
the Middle Permian Huang Yang Ling group
tectono magmatic rock
low-temperature hydrothermal deposit
