摘要
猴家沟地区大地构造位置位于祁连-北秦岭加里东造山带接合部位,区域上韧性断裂构造发育,岩浆活动频繁,具有良好的成矿地质背景条件。
The Houjiagou area is located at the juncture of Caledonian Orogenic belt in Qilian and north Qin Mountains,where ductile and ductile-brittle faults are well developed,magmatism is frequent,hydrothermal activity and wall rock alteration are strong,the ore-forming geological background conditions are favorable.
作者
李晨
罗二刚
谢冰冰
LI Chen;LUO Er-gang;XIE Bing-bing(Gansu Non-ferrous Metal Geological Exploration Bureau Tianshui Mineral Exploration Institute,Tianshui 741025,China)
出处
《甘肃冶金》
2021年第3期98-101,共4页
Gansu Metallurgy
关键词
地质特征
矿体成因
金矿
猴家沟
geological features
orebody genesis
gold deposit
Houjiagou
