Multispectral remote sensing expression of lineaments and alteration minerals in part of crystalline rock units of Southwestern Nigeria: Implication on gold prospecting

Kazeem Oladimeji Olomo , Muriana Zaid Mohammed , Oluwatoyin Khadijat Olomo , Omowumi Ademila , Marvelous Ayomide Dadamu
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Abstract

The Ilesha schist belt, the location of the research area, comprises one of Nigeria's most notable schist belts, which has attracted attention due to its considerable mineral resources, including gold deposits. Recent studies in the region have emphasized aerogeophysical mapping of geological features and the implication this has for mineral potential. However, various types of alteration and their relationships with gold deposits in the region have not received proper consideration. This research is aimed at identifying specific type of hydrothermal alteration associated with existing gold deposits in the study area as a reference to establishing new prospective zones and producing mineral prospect map of the area. To achieve this, Landsat Enhanced Thematic Mapper plus (Landsat-7 ETM+), and Advanced Space borne Thermal Emission and Reflection Radiometer (ASTER) data were utilized to define the association of lineaments and propylitic, phyllic, and argillic alteration types with Gold deposit within the study area. The processing of Landsat-7 ETM+ data were aided by applying Band ratio procedure and Principal Component Analysis (PCA). The validation was carried out using the active mining site of the study area, X-ray diffraction (XRD) analysis of some rock samples and electrical resistivity method. The results were integrated to provide information on lineaments, alteration minerals, and different types of hydrothermal alteration within the study area. Processed Landsat-7 ETM+ data delineated the structural elements as lineaments synonymous to lithologic contacts and faults/fracture zones, trending NE–SW direction, most probably controlling the alteration zones formation, distribution and localization of mineral in the country rocks of the belt. The Band ratio procedure and Principal Component Analysis (PCA) also showed that the area is rich in alteration minerals, particularly ferrous, ferric and clay minerals. ASTER multispectral analysis gave an imprint of the key alteration types within the study area, with phyllic alterations being noticeably the major alteration type associated with Gold deposits, and poses the highest prospective zone for Gold occurrence in the study area. Validation of the observed lineament dense areas with Vertical Electrical Sounding (VES) revealed highly fracture zones, thereby validating the structural framework of the study area. Also, spatial analysis involving percentage correlation evaluation carried out to compute the spatial connection between gold locations and altered zones showed that gold mine pits strongly matched with mapped altered zones with 85 percent correlation. Lastly, mineral compositions of the altered zones were confirmed by X-ray diffraction (XRD) analysis of the analyzed samples collected within the area. The research helped in understanding the spatial distribution of gold mineralisation within the study area. It is recommended that exploitation efforts be expanded to the delineated phyllic and propylitic altered zones in North, Northwestern and Northeastern part of the study area. These regions are the new probable promising site for gold potential.
奈及利亚西南部部分结晶岩单元中地貌与蚀变矿物的多光谱遥感表达及其找金意义
Ilesha片岩带是尼日利亚最著名的片岩带之一,由于其丰富的矿产资源(包括金矿)而引起了人们的关注。该地区最近的研究强调了地质特征的航空地球物理制图及其对矿产潜力的影响。然而,对该地区各种蚀变类型及其与金矿床的关系研究还不够深入。本研究旨在识别研究区内与现有金矿床相关的特定热液蚀变类型,为该区建立新的找矿带和制作找矿图提供参考。为了实现这一目标,利用Landsat增强型专题绘图器plus (Landsat-7 ETM+)和先进的星载热发射和反射辐射仪(ASTER)数据来确定研究区域内的地貌和丙基、叶状和泥质蚀变类型与金矿床的关联。利用波段比法和主成分分析法(PCA)对Landsat-7卫星ETM+数据进行处理。利用研究区活动矿区、部分岩样的x射线衍射(XRD)分析和电阻率法进行了验证。综合研究结果,提供了研究区内的地貌、蚀变矿物和不同类型热液蚀变的信息。经处理的Landsat-7 ETM+数据将构造元素圈定为与岩性接触和断裂/破裂带同属的线状,呈NE-SW向,很可能控制着带内围岩蚀变带的形成、分布和矿物定位。带比分析和主成分分析表明,该区蚀变矿物丰富,以亚铁、铁和粘土矿物为主。ASTER多光谱分析对研究区内的主要蚀变类型进行了标记,其中层状蚀变是与金矿床相关的主要蚀变类型,是研究区黄金找矿远景区。利用垂直电测深(VES)对观测到的密集区域进行验证,发现了高度断裂带,从而验证了研究区的构造框架。同时,利用空间相关性分析方法计算了金矿位置与蚀变带之间的空间联系,结果表明,金矿矿坑与已测绘的蚀变带具有很强的匹配性,相关性达85%。最后,通过x射线衍射(XRD)对该区域内采集的分析样品进行分析,确定了蚀变带的矿物组成。该研究有助于了解研究区内金矿化的空间分布。建议将开发范围扩大到研究区北部、西北部和东北部已圈定的绿、丙基蚀变带。这些地区是新的可能有金矿潜力的地点。
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