摘要
老道沟铜多金属矿床位于大兴安岭南段乌兰浩特-黄岗梁多金属成矿带东侧的铜多金属成矿带,在1∶1万土壤化探测量和1∶1万激电中梯测量的基础上,经过工程验证,圈定多条铜多金属矿(化)体。矿床为裂隙充填交代型,成矿明显受构造岩浆活动控制,区域与成矿地质特征显示老道沟地区具有良好的铜多金属矿找矿前景。
Laodaogou copper - polymetallic deposit is located at east part of Wulanhaote - Huanggangliang metallogenic belt. On the basis of 1 ： 10000 soil geochemical and 1 ： 10000 IP induced - current middle - gradi- ent surveys and surface geological engineering, several copper- polymetallic ore bodies were outlied. The ore deposit is formed by fracture filling and metasometism and controlled by tectonomagamatism. All regional and metallogenic features show that the Laodaogou area have good exploration prospects.
出处
《内蒙古工业大学学报（自然科学版）》
2012年第1期47-51,共5页
Journal of Inner Mongolia University of Technology：Natural Science Edition
关键词
找矿潜力
化探铜多金属矿
内蒙古老道沟
metallogenic potential, geochemical prospecting, copper - polymetallic deposit, Inner Mon-golia Laodaogou.
