综合电(磁)法在内蒙古希热哈达勘查区金多金属矿勘查的应用

    Application of comprehensive electric (magnetic) method in the exploration of gold polymetallic deposits in Xirehada exploration area of Inner Mongolia

    • 摘要: 内蒙古北山希热哈达勘查区具有良好的金多金属矿找矿潜力,为查明该区地质构造格架、断裂、岩体等控矿要素的分布特征,更好地指导详查工作布设并圈定找矿靶区,在研究区开展了激电中梯、激电测深和音频大地电磁(audio-magnetotellurics, AMT)测深综合电(磁)法的应用研究。研究结果显示: 激电中梯异常特征反映研究区存在4条NWW向断裂F1、F2、F3及F4,圈定与断裂相关的3个异常区IP1、IP2及IP3,音频大地电磁测深异常特征反映断裂构造的空间展布特征为F1、F2、F3断裂倾向北东,F4断裂倾向南西,激电测深进一步反映出F3断裂的产状和成矿有利区的埋深特征。经过探槽工程的验证,在IP2异常区识别一条金矿脉,取得了良好的找矿效果。研究基本建立了一套厚覆盖区的电(磁)法找矿勘探方法,可为在浅表芒硝层开展激电测深工作提供借鉴。多种物探方法的综合应用能大致推断出构造及矿体的深部展布特征,同时也缩小了找矿的有利区域,为下一步地质钻探工作提供依据。

       

      Abstract: Xirehada exploration area in Beishan of Inner Mongolia has great potential for gold polymetallic deposit prospecting. In order to identify the distribution characteristics of ore controlling elements such as geological structure framework, faults, and rock masses in the area, and better guide the detailed survey work and delineate the prospecting target area, the authors applied comprehensive electrical (magnetic) methods such as induced polarization middle gradient, induced polarization sounding, and audio magnetotelluric sounding in the study area. The research results show that the anomalous features of the induced polarization gradient reflected the existence of four NWW oriented fault structures F1, F2, F3, and F4, and three related anomaly areas IP1, IP2, and IP3 were delineated. The anomalous features of the audio magnetotelluric sounding reflected the spatial distribution characteristics of the fault structures F1, F2, and F3 dipping to the northeast, and F4 dipping to the southwest. The induced polarization sounding further reflected the occurrence of the fault structure F3 and the burial depth characteristics of the favorable mineralization area. After verification by the trench engineering, a gold vein was identified in IP2 anomaly area, and good prospecting results were achieved. A set of electric (magnetic) exploration methods for thick coverage areas was established, providing references for conducting induced polarization soun-ding in shallow saltpeter layers. The deep distribution characteristics of structures and ore bodies can be roughly inferred by comprehensive application of multiple geophysical methods. Meanwhile, the favorable areas for mineral exploration were also reduced, providing basis for the geological drilling work in the future.

       

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