获各琦铜矿一号矿床地质特征及找矿方向探讨  

Discussion on geological features and prospecting direction of No.1 deposit in Huogeqi Copper Mine

作　　者：王寿林[1] 钟世杰[1] 霍红亮[1] 

机构地区：[1]巴彦淖尔西部铜业有限公司,内蒙古巴彦淖尔015000

出　　处：《有色金属（矿山部分）》2012年第2期43-47,共5页NONFERROUS METALS(Mining Section）

摘　　要：通过对获各琦铜矿区域地质背景和矿床地质特征分析研究,概括获各琦铜矿地质特征如下:矿床严格受断裂构造和地层控制;岩浆活动强烈,对成矿起决定作用;矿体形态呈层状、似层状;具有分枝复合现象。并通过对一号矿床生产地质资料以及矿区构造的研究,结合生产地质勘探成果,认为一号矿床深边部具有很大的找矿潜力。Based on the analysis on geological background and geological characteristics of deposit,geological features of Huogeqi Copper Mine are summarized as following： 1） The deposits are strictly controlled by fault structures and strata.2） Strong magma activity is decisive to ore-forming.3） Ore body with the branch-complex phenomenon presents with layered structure and lay-like structure.Through study on geological data and structures of No.1 deposit,and combining with the former exploration achievements,the deep and neighbouring regions of No.1 deposit are supposed to be focused on.

关 键 词：获各琦铜矿 一号矿床 地质特征 找矿方向 

分 类 号：TD15[矿业工程—矿山地质测量]