摘要
哈尔楚鲁图铜银铅锌矿位于内蒙古赤峰市的克什克腾旗北部,区域所在的大兴安岭中南段地区是我国重要的铜多金属矿床集区之一。该区域成矿地质条件优越,具有良好的区域成矿地质前景。研究表明:矿床为中-低温热液充填式脉状铅锌多金属矿,矿石类型为金属硫化物;以近矿围岩蚀变为直接找矿标志通过系统野外地质工作发现的76个矿体表明,成矿具有深部隐伏,严格受构造控制,沿构造平行展布的规律特点。
The copper,silver,lead and zinc deposit in Harzhulutu is located in the northern part of the Hexigten Banner of Chifeng,Inner Mongolia.The metallogenic geological conditions of this area are superior,and it has a good regional metallogenic geological prospect.The study shows that the deposit is a vein-shaped lead-zinc polymetallic deposit filled with mesothermal-low temperature hydrothermal solution,and the ore type is a metal sulfide,the mineralization is deep concealed,strictly controlled by the structure and distributed parallel to the structure.
作者
吴云雷
卢守卿
张迎年
曹宇岗
常晓磊
WU Yun-lei;LU Shou-qing;ZHANG Ying-nian;CAO Yu-gang;CHANG Xiao-lei(N0.1 Institute of Geological and Mineral Resources Exploration of Henan,Zhengzhou 450001,China)
出处
《世界有色金属》
2020年第13期78-79,共2页
World Nonferrous Metals
关键词
铜银铅锌矿
近矿围岩蚀变
隐伏矿体
Cu-Ag-Pb-Zn deposit
Adjacent wall rock alteration
Concealed orebody