摘要
多期的造山作用,使该区的构造变形更加复杂化,由此亦伴随着不同程度的变质作用和热液成矿作用,黄土岭矿区及其周边的铅锌矿床,在宏观上即为上述构造变动、变质作用和热液活动的综合产物。
The tectonic deformation of this area is complicated by the multi-stage orogeny,which is accompanied by different degree of metamorphism and hydrothermal mineralization.The lead-zinc deposit in the Huangtuling mining area and its surrounding area is a comprehensive product of the above mentioned tectonic changes,metamorphism and hydrothermal.
作者
屈笑冬
高向玲
QU Xiao-dong;GAO Xiang-ling(Northwest Institute of mining and metallurgy,Baiyin 730900,China)
出处
《世界有色金属》
2020年第8期118-119,共2页
World Nonferrous Metals
关键词
地质构造
热液活动
铅锌矿床
镇安
geologic(al)structure
Hydrothermal activity
lead and zinc deposit
Zhenan
