摘要
切列克其铁矿床是上世纪50年代末发现的一处铁矿产地。从2004年起至今,通过大量深入细致的地质勘查工作,已基本查明矿区矿体数量,分布的范围,矿体特征,埋深,从现有成果看,该矿床类型已经成为一处大型沉积型铁矿床。由于探边摸底的工作还未最终完成,矿床深部还有很大的增储潜力,为下一步找矿指明了方向。
Cut column g of its iron ore deposit is found in the late 1950 s, an iron ore producer.Since 2004, through a large number Of detailed geological exploration work, has been basically identified number of orebody mining area, the scope of distribution, orebody characteristics, burial depth, from the existing achievements, this type of deposit has become a large deposit type iron ore deposit.Due to the delineation to find work is not finished, deep and great potential for the basis of ore deposits, pointed out the direction for further prospecting.
出处
《世界有色金属》
2017年第1期222-222,224,共2页
World Nonferrous Metals
关键词
切列克其铁矿
矿床
地质特征
Qieliekeqi iron ore deposit
geological characteristics