摘要
西昆仑康西瓦一带是新疆重要的铅锌矿成矿带,位于新疆西南部地区,三江造山系(西藏)以及塔什库尔干-甜水海地块(羌塘弧盆系)与羌北地块是该矿的大地构造所在,康西瓦-大红柳滩断裂在其北部方向上进行展布。断裂、褶皱构造极其发育。近年来,随着地质研究工作的不断深入,在该区已经发现多处铅锌矿(床)点和铁、铜矿,显示该区巨大的找矿潜力。基于此,文中笔者结合前人研究成果,对西昆仑康西瓦一带铅锌矿成矿规律与找矿前景展开探讨,以期为相关工作提供借鉴于参考。
The West Kunlun KANGXIWA area in Xinjiang is an important metallogenic belt,located in the southwest of Xinjiang area,the Sanjiang orogenic system(Tibet)and Tashikuergan(Qiangtang Tianshuihai block arc basin system)and the northern Qiangtang massif is the tectonic ore of KANGXIWA-fracture distribution in the red beach the northern direction.Fracture and fold structure are extremely developed.In recent years,showing the great prospecting potential in this area.Based on the previous research results,the author in this paper,on the West Kunlun area of KANGXIWA metallogenic regularity and prospecting prospect,in order to provide reference to the reference for related work.
作者
李崔刚
赵立元
LI Cui-gang;ZHAO Li-yuan(Xinjiang geological and Mining Bureau second zone adjustment Brigade,Changji 831100,China)
出处
《世界有色金属》
2018年第1期113-113,115,共2页
World Nonferrous Metals
关键词
西昆仑
铅锌矿
康西瓦一带
成矿特征
找矿分析
West Kunlun
lead-zinc deposit
KANGXIWA area
metallogenic characteristics
Prospecting Analysis
