尼日利亚西南部Ilesha片岩带部分中温金矿床航磁填图及放射性元素对矿物组成的影响

K. O. Olomo, S. Bayode, O. A. Alagbe, G. Olayanju, Oluwatoyin Khadijat Olaleye
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引用次数: 1

摘要

对尼日利亚西南部Ilesha片岩带西部中温蚀变带相关的潜在金矿化的航空磁和辐射测量数据集进行了解释。这样做是为了提供有关该地区伴随金矿化的地质变化可能程度的信息。伽玛谱解释数据成功地圈定了与钾钾富集有关的热液蚀变带,并将其作为金矿的靶区。承载矿床的地质构造特征被识别为由岩性接触和断层/裂缝代表的线条,这些线条成功地从航空磁数据中提取出来。为了增强研究区域岩石的钾元素特征,计算了钾元素偏差(KD)图。因此,KD图代表了整个研究区内真实的钾分布,这些钾来自热液蚀变,其中的热液化带显示出高KD值。利用一阶垂直导数(FVD)和总水平梯度(THG)图来圈定轮廓。用两个主要线性集的频率上升图将这些线性集连接起来;观察到主要和次要的轮廓。三维欧拉反褶积(EUD)方法也被应用于THG图,以定位和评估地下结构的深度。采用构造指数为0 (si = 0)建模的堤坝和触点的最佳三维EUD解决方案用于估计研究区域300至700 m异常源的深度。EUD结果还揭示了几个隐藏在研究区现有地质图中的地下构造。通过综合研究区磁线和蚀变带图,绘制了一幅远景矿化图,显示了可能的高矿产资源区。已发现的热液蚀变带地质构造与已知金矿坑的叠加关系密切。
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Aeromagnetic Mapping and Radioelement Influence on Mineralogical Composition of Mesothermal Gold Deposit in Part of Ilesha Schist Belt, Southwestern Nigeria
ABSTRACT Airborne magnetic and radiometry data sets over potential gold mineralisation associated with mesothermal alteration zones in the western Ilesha schist belt, Southwestern Nigeria, were interpreted. This was done to provide information on possible extent of geologic transformations that accompanied gold mineralisation in the area. Interpreted gamma spectrometric data were successfully used in delineating zones of hydrothermal alteration associated with potassium K enrichment as the target for gold deposits. The geological structural features that host the ore deposits were identified as lineament represented by lithological contacts and faults/fractures that were successfully exacted from the airborne magnetic data. The potassium deviation (KD) map was computed to enhance the potassium signature of rocks in the area of study. Thus, the KD map represents real potassium distribution across the study area emanated from hydrothermal alteration where hydrothermalised zones were displayed by high KD values. First vertical derivative (FVD) and total horizontal gradient (THG) maps were used to delineate lineaments. These lineaments were connected using the frequency rose diagram with two main lineament set,; major and minor lineaments observed. The 3D Euler deconvolution (EUD) method was also applied on the THG map to locate and evaluate depths to subsurface structures. The best 3D EUD solution for dykes and contacts modelled using the Structural Index of zero (S.I = 0) was used to estimate the depth to these anomaly sources at 300 to 700 m in the study area. The EUD results also revealed several subsurface structures which were hidden in the existing geological map of the study area. A prospective mineralisation map was produced from the synthesis of both magnetic lineaments and alteration zones maps derived for the study area, showing the areas of probable high mineral resources. Strong relationships were observed between the mapped hydrothermal altered zoneseologic structures and superimpose known gold mining pits.
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