GROUND MAGNETIC STUDY OF GEOLOGICAL STRUCTURES AND MINERALIZATION IN AWO AREA, NEAR EDE, SOUTH WESTERN NIGERIA

W. Igboama, M. Aroyehun, J. A. Olowofela, O. Hammed, N. Ugwu
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Abstract

Ground magnetic study was carried out in Awo area, Osun State, Nigeria. The area lies within latitudes 70 44¢N and 70 48¢N and longitudes 4020¢E and 4024¢E in Southwestern part of Nigeria. The study focused on delineation of geological structures like: faults, fractures and possible minerals in the area.  GM122 Proton Precession magnetometer was employed and 16 traverses were executed along roads and pathways for ease of labour and adequate coverage at spacing interval of 10 m between station points. Isolation of residuals was carried out to get magnetic residual intensity values that were plotted against station points using Microsoft excel. The quantitative interpretation was done using “half-slope” and “straight-slope” methods, as they are easy to use, fast and cost effective. The range of overburden thickness to the top of magnetized body obtained was between 2.50 and 30.00 metres. Qualitatively, the results obtained were used to delineate inflection points, contacts, fractures and faults by plotting 2-D and 3-D contour maps using Sufer applications. The graphs indicate geological structures, rock types and magnetic characteristics of minerals. The low magnetic values suggest presence of faults and fractures in the area while the high relative intensity values indicate deep structures, which may be due to block faulting. These findings have significant implications for mineral exploration in the region, particularly for identifying structurally controlled deposits. Rock types including banded gneiss and granite gneiss with pegmatite veins and economically valuable minerals such as tantalite, barite, quartz, mica and gravel were found in the area.
尼日利亚西南部埃德附近阿沃地区地质结构和矿化的地磁研究
地磁研究在尼日利亚奥苏恩州的阿沃地区进行。该地区位于尼日利亚西南部,北纬 70 44¢ 和 70 48¢,东经 4020¢ 和 4024¢。研究重点是划定该地区的地质结构,如断层、裂缝和可能的矿物。 使用了 GM122 质子前驱磁强计,并沿道路和小径进行了 16 次穿越,以方便劳动和充分覆盖,站点之间的间距为 10 米。对残差进行了隔离,以获得磁残差强度值,并使用 Microsoft excel 根据测站点绘制出图。由于 "半坡法 "和 "直坡法 "易于使用、快速且成本效益高,因此采用这两种方法进行定量解释。从覆盖层厚度到磁化体顶部的范围为 2.50 米至 30.00 米。在定性方面,使用 Sufer 应用程序绘制二维和三维等高线图,利用获得的结果来划分拐点、接触点、断裂和断层。这些图显示了地质结构、岩石类型和矿物的磁性特征。低磁性值表明该地区存在断层和裂缝,而高相对强度值则表明深层结构,这可能是由于块状断层造成的。这些发现对该地区的矿产勘探具有重要意义,尤其是在确定受构造控制的矿藏方面。在该地区发现的岩石类型包括带状片麻岩和花岗片麻岩,并伴有伟晶岩脉和具有经济价值的矿物,如钽铁矿、重晶石、石英、云母和砾石。
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