摘要
太平金矿受奥陶系、花岗斑岩及硅化破碎带控制，矿体呈脉状、透镜状，具埋藏浅特点。金来源于地幔、地层及岩体，矿床成因属与花岗斑岩有关的低温热液金矿床。
Taiping gold deposit is controlled by Ordovician strata,granite porphyry and silicified crush belt,It is a shallow buried deposit,orebodies occur vein and lenticular,Au origins from the mantle,strata and lithosomes,The deposit genesis is the microthermal hydrothermal diposit which is related with the granite porprhyry
出处
《湖南地质》
1999年第2期112-115,共4页
Hunan Geology
关键词
金矿床
地质特征
矿床成因
安化县
太平乡
Gold deposit,Geological characteristics,Deposit genesis,Anhua,Taiping
