Resolving Optimum Magnetic Signatures for Drill-Hole Targeting in Gold Exploration – A Case Study for Mbudzane in Gwanda, Zimbabwe

D. J. Hlatywayo, E. Sakala
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Abstract

Optimum magnetic signatures for drill-hole targeting in gold exploration in Mbudzane were resolved from induced polarisation-resistivity and magnetic anomalies. Total magnetic field and a gold-in-soil map showed the area is magnetically quiet with high anomalous values along old gold workings. Induced polarisation was carried out along a grid for lines of 500m length, 50m separation and a baseline oriented at 330˚. The survey comprised a gradient array and three real sections. The magnetic survey was conducted over the same grid as the induced polarisation. Stations were set at 5m intervals for a line spacing of 50m. The results show intense anomalies that suggest different degrees of magnetic alteration and a set of conjugate lineaments and faults that possibly control the mineralisation in Mbudzane. The tilt derivative of the reduced-to-pole image resolves the separation between anomalies, giving information on the faulting. High chargeability is confined to the sheared and silicified mafic schist. The gradient resistivity image revealed contact between rock formations. Real section IP shows coincident low chargeability – low resistivity anomalies close to the surface. Chargeability intensity increases with depth, suggesting incipient development of disseminated sulphide replacement zones. A strong correlation between ground magnetic inferred contacts and apparent resistivity-chargeability anomalies forms the basis for suggesting a new drill-hole targeting. They dictate both the depth and angle at which drilling should be carried out. These results should be applicable to any region where drill-hole targeting in gold exploration may be required.
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金矿找矿中钻孔定位的最佳磁特征求解——以津巴布韦Gwanda Mbudzane为例
利用感应极化电阻率和磁异常,求解了Mbudzane金矿找矿钻孔定位的最佳磁特征。总磁场和土壤中含金图显示,该地区的磁场很安静,沿旧金矿工作区有高异常值。诱导极化沿一个500米长、50米间距、330˚取向基线的网格进行。测量包括一个梯度阵列和三个实际剖面。磁测量是在感应极化的同一网格上进行的。每隔5米设置车站,线间距为50米。结果显示强烈的异常表明不同程度的磁蚀变和一组可能控制Mbudzane矿化的共轭地貌和断层。简化到极点图像的倾斜导数解决了异常之间的分离问题,提供了断层的信息。高荷电性仅限于剪切硅化镁质片岩。梯度电阻率图像揭示了岩层之间的接触。真实剖面IP显示接近地表的低电荷率-低电阻率异常。电荷强度随深度增加而增加,表明浸染型硫化物替代带已开始发育。推断出的地磁接触与视电阻率-电荷率异常之间的强烈相关性,为提出新的钻孔定位奠定了基础。它们规定了钻孔的深度和角度。这些结果应该适用于任何地区,在黄金勘探中可能需要钻孔定位。
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