摘要
茶棚银矿区位于华北地台北缘,区域内构造-岩浆活动强烈,主要为燕山期中酸性岩浆活动。茶棚银矿成因类型应属与火山—次火山作用有关的浅成低温热液型矿床。
The Chapeng silver deposit is located in the northern margin of the north China Platform.The tectonomagmatic activity in the area is strong,and the main activity is intermediate-acid magmatism in Yan Mountains.The Genesis of the Chapeng silver deposit belongs to the epithermal type related to the subvolcanism.
作者
唐绍金
TANG Shao-jin(Second Geological Brigade,Hebei Provincial Bureau of Geology and Mineral Resources,Tangshan 063000,China)
出处
《世界有色金属》
2019年第19期94-95,共2页
World Nonferrous Metals
