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金属矿山 ›› 2020, Vol. 49 ›› Issue (04): 118-129.

• 地质与测量 • 上一篇    下一篇

内蒙古维拉斯托矿区隐伏矿体大功率激电综合找矿勘查

占文锋 王 强 刘太福   

  1. 北京工业职业技术学院建筑与测绘工程学院,北京 100042
  • 出版日期:2020-04-15 发布日期:2020-04-30
  • 基金资助:

    北京市教育委员会科技计划项目(编号:KM201810853006),北京高校校际联合课题资助项目(编号:BGY2018JF—207)。

Integrated Exploration of Concealed Orebody by High-power Induced Polarization in Weilasituo Mining Area,Inner Mongolia

Zhan Wenfeng Wang Qiang Liu Taifu   

  1. School of Architectural and Surveying & Mapping Engineering,Beijing Polytechnic College,Beijing 100042,China
  • Online:2020-04-15 Published:2020-04-30

摘要:  维拉斯托岩浆热液型铜锌多金属矿床位于大兴安岭成矿带南段,已探明矿石量超过800万t,资源潜力巨大。矿体主要赋存于下元古界锡林郭勒杂岩内,受NE向断裂带控制,地表为第四系覆盖,覆盖区隐伏矿体的准确定位是当前亟待解决的问题。通过详细分析研究区地质资料、钻孔资料、物性资料及地面高精度磁测资料,对找矿潜力较大的物探异常区进行了激电扫面、剖面和测深工作,并对测量数据进行了深入的解译分析。结果表明:①研究区辉长岩的磁化率及剩余磁化强度较大,其余岩性无明显的磁性变化,围岩、侵入岩、构造岩(包括蚀变的)以及氧化矿等均不会产生激电异常,视极化率低于4%,视电阻率基本大于1 000 Ω·m,矿体是引起异常的主要原因,其视极化率小于4%,视电阻率约1 000 Ω·m,呈高极化、中—低阻特征,以此作为研究区激电异常划分的依据;②平面视极化率、视电阻率显示两条SN向高值带,近于平行排列,平面上呈“S”形展布,构成了区内的基本格局,其间展布的NE、NW向高值带相互交织成网格状,节点位置即为异常点,推断为矿体富集的主要区位,据此将区内异常划分为东西两个条带,沿南北方向可进一步划分为4个异常区;③对典型的激电测深剖面进行了解译和反演,发现反演结果与实测揭露的异常体所在的平面位置基本吻合,但反演的深度略浅;在异常位置通过布设钻孔验证,见矿效果较好,对各靶区下一步钻孔布设具有重要的指导意义。上述分析表明:所采用的物探综合勘查方法和资料解译方法具有较好的可行性,在类似地区具有一定的运用前景。

关键词: 铜锌多金属矿, 深部找矿, 维拉斯托矿区 , 隐伏矿体 , 大功率激电测量

Abstract: The Weilasituo magmatic hydrothermal Cu-Zn polymetallic deposit is located in the southern section of the Great Khingan metallogenic belt,more than 8 million tons of ores have been found,which has great potential for resources.The orebodies are mainly occurred in the Xilinguole complex rocks of the Lower Proterozoic and controlled by NE-trending faults.The surface is covered by Quaternary sediments,and accurate location of concealed orebodies in this overburden area is an urgent problem to be solved.Combining with the geological data,borehole data,physical property data and ground high-precision magnetic survey data,the work of induced polarization (IP) sweep,profile and IP sounding are carried out in the geophysical anomaly area with great prospecting potential,the measurement data is interpreted and analyzed in depth.The results show that:①The magnetic susceptibility and residual magnetization of gabbro are relatively large,the other lithologlies have no obvious magnetic changes in the study area,the surrounding rocks,intrusive rocks,tectonites (including alteration) and oxidized ores can not produce IP anomalies,the apparent polarizability is less than 4%,which apparent resistivity is greater than 1 000 Ω?m.Orebody is the main cause of IP anomalies,which apparent polarizability is higher than 4% and the apparent resistivity is about 1 000 Ω?m,which can be used as the basis of dividing IP anomalies in survey area.②The apparent polarizability and apparent resistivity contour maps show that two high value zones are distributed in North-South direction,which are distributed in nearly parallel and spread in a "S" shape on the plane,thus constituting the basic pattern of the study area,and the NE and NW orientation high value zones are distributed and interlaced into grids,the positions of nodes are the IP abnormal points,which can be inferred as the main location of orebody enrichment.Accordingly,anomalies in the survey area can be divided into the east belt and the west belt,and further divided into four anomalous zones along the North-South direction.③Through the interpretation and inversion of IP sounding profiles,the plane position of the anomalous bodies revealed by the interpretation of the inversion results is basically consistent with the ones obtained by actual measurement,but the inversion depth is slightly shallow.Boreholes are laid in the anomalous areas,the orebodies are exposed effectively,which has important guiding significance for the further boreholes layout in the study area.The above analysis further indicated that the integrated geophysical prospecting method and data interpretation method are feasible,which can be used in the similar areas.

Key words: Cu-Zn polymetallic deposit, Deep prospecting, Weilasituo mining area, Concealed orebody, High-power induced polarization