摘要
该金矿位于中朝准地台北部,区内构造发育,构造岩浆活动强烈。地层以太古界单塔子群凤凰咀组为主,矿体赋存于太古界单塔子群凤凰咀组变质岩中,矿床形态呈细脉状或透镜状产出。矿床的成因属中低温热液石英脉型金矿床。
The gold deposit is located in the northern part of the sino-korean paraplatform platform.The main stratum is Fenghuangzui formation of Archean Single Tazi group.The ore bodies occur in metamorphic rocks of Fenghuangzui formation of Archean Single Tazi group.The Genesis of the deposit is a Mesothermal quartz vein type gold deposit.
作者
于婷婷
YU Ting-ting(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113-113,115,共2页
World Nonferrous Metals
关键词
丰宁
金矿
构造
低温热液
fengning
gold deposit
structure
low temperature hydrothermal solution
