摘要
富蕴县翁格尔阔腊北金矿是阿尔泰铜、银、金多金属成矿带中规模较大的金矿点,出露地层主要为晚古生界泥盆系、石炭系地层,钙质绢云千枚岩、蚀变粉砂质板岩、钙质绿泥絹云千枚岩地层为金的矿源层。通过对矿区地质特征及成矿模式分析,翁格尔阔腊北金矿是在近地表环境中形成的浅成低温热液型金矿床。
Fuyun County Hongre broad North La gold deposit is a larger size in Altai gold copper,silver and gold polymetallic metallogenic belt,the exposed strata in the late Paleozoic Devonian and Carboniferous strata,calcareous sericite phyllite,altered silty slate,calcareous chlorite sericite phyllite stratum for ore source the layer of gold.Through the analysis of the geological characteristics and metallogenic model of the mining area,the Weng Guer North gold deposit is an epithermal gold deposit formed in the near surface environment.
作者
黄伟
HUANG Wei(Fourth Geological Team of the Xinjiang Uygur Autonomous Region geological and mineral exploration and Development Bureau, Aletai 836500,China)
出处
《世界有色金属》
2018年第1期145-145,147,共2页
World Nonferrous Metals
关键词
翁格尔阔腊北
金矿
地质特征
矿床成因
Unger Kuo La north
gold deposit
geological characteristics
genesis of the deposit