摘要
后底洞金矿床产于二叠纪柯岛组变质岩系与华力西期辉长岩体内外接触带。矿化类型为含金蚀变岩型 ,矿体受北东向断裂构造控制 ,矿床成因类型为次火山热液型。
The Houdidong Au deposit occurred in the Permian, Kedao Formation contact zone between metamorphic rock series and Variscan gabbro body. The mineralized type belongs to gold-bearing altered rock one, ore body is controlled by faulted structure with NE strike. The genetic type of deposit is subvolcanic hydrothermal one.
出处
《吉林地质》
2001年第3期18-22,共5页
Jilin Geology
关键词
金矿床
地质特征
找矿思路
吉林
金矿化
断裂构造
Au deposit
geologic features
the train of thought for prospecting
Houdidong
