Application of electrical resistivity tomography for mapping gold mineralization potential in Iperindo, Ilesha schist belt, southwestern Nigeria

Olawale OlakunleOsinowo, A. Usman, Ayotunde Allen Omitoogun
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引用次数: 1

Abstract

This study applied Electrical Resistivity Tomography geophysical investigation technique to evaluate the gold mineralization potential of Iperindo in Ilesha Schist Belt, southwestern Nigeria, where commercial exploitation capable of generating revenue and employment for the inhabitants has been challenged by lack / inadequate subsurface geological/geophysical information. The filtered and inverted electrical resistivity data acquired through five (5) 336 m long E – W trending profiles, established 10 m apart from each other, delineate isolated near surface but thick (> 30 m) low resistivity zones, especially at the eastern and western ends of the study area. Some of the delineated low resistivity zones (3 – 200 𝛀m) present vertical sharp edges, likely created by vertical faults that flank the zones on both sides. The low resistivity of these zones could be attributed to the occurrence of conductive material such as gold and associated base metals which probably exist in pegmatitic veins within the zones.   
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电阻率层析成像在尼日利亚西南部Ilesha片岩带Iperindo金矿化潜力勘查中的应用
本研究应用电阻率层析物探技术评估了尼日利亚西南部Ilesha片岩带Iperindo的金矿化潜力。由于地下地质/地球物理信息缺乏/不足,该地区能够为居民创造收入和就业的商业开采受到了挑战。通过建立5条长336 m的E - W向剖面,并相互间隔10 m,滤波反演得到的电阻率数据,圈定了孤立的近地表但较厚(> 30 m)的低电阻率带,特别是在研究区东端和西端。一些描绘的低电阻率带(3 - 200𝛀m)呈现垂直的尖锐边缘,可能是由两侧的垂直断层造成的。这些带的低电阻率可能是由于在带内的辉长岩脉中可能存在金及其伴生贱金属等导电物质所致。
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