新疆含金属石英脉的成因及地质特征  

Genesis and geological characteristics of Quartz vein containing metal deposits IN Xinjiang

作　　者：兰飞 张自凯 管志荣[1] LAN Fei;ZHANG Zi-kai;GUAN Zhi-rong(Chengdu University of Technology,Chengdu 610059,China)

机构地区：[1]成都理工大学,四川成都610059

出　　处：《世界有色金属》2018年第11期184-185,共2页World Nonferrous Metals

摘　　要：随着工业对金属矿石的需求日益增高,金属矿石的地位越来越重要,在高科技领域具有无可替代的作用。而石英化学成分的细微变化又是矿物形成时的地质物理化学条件的标志,它蕴藏有大量的成因信息和找矿信息。不同环境的金属矿石,其成因也不尽相同。通过对比分析得出其布提沟的含金属石英脉是充填在裂隙,又经过后期构造作用形成。With the increasing demand for metal ores in the industry,the status of metal ore is becoming more and more important,and plays an irreplaceable role in the field of high technology.The genesis of metallic ores in different environments is different.Through comparison and analysis,it is concluded that the metal minerals in the Bu Ti ditch are filled with fissures and formed by late tectonic action.

关 键 词：矿床 容矿构造 低温热液 

分 类 号：P618.51[天文地球—矿床学]