伊利沙片岩带金矿热液蚀变带斑岩型铜金钼矿床的多方面研究

K. O. Olomo, S. Bayode, O. A. Alagbe, G. Olayanju, Oluwatoyin Khadijat Olaleye
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引用次数: 2

摘要

本研究的目的是绘制尼日利亚西南部Ilesha片岩带内斑岩系统的分布图,以便于商业金矿以及铜和钼矿床的可及性,以促进该地区的开采活动。利用了该地区的航空磁和辐射数据。通过赤道还原、垂直导数、解析信号和谱分析,增强了获得的磁场总磁场强度图。研究区增强总磁强图显示,在深度306 ~ 421 m范围内与铜、金、钼矿床伴生隐伏侵入岩有关的磁异常。垂直导数图显示南部和西部有浅层磁体,为铜、金、钼矿床的可能带。分析信号图显示,在0.1 nT/M ~ 1.7 nT/M之间的高强度磁带突出显示了含斑岩的基底断块。航空辐射测量图像显示了不同岩性的放射性元素分布。部分地区钾离子浓度较高,显示有利于铜、金、钼矿床富集的热液蚀变带。Th/k比值计算和复合钾图增强了与热液蚀变带相关的钾富集特征。利用地球化学分析对航空结果进行验证,证实在已测绘的热液蚀变带内存在铜-金-钼元素。这项研究已查明其他有价值的矿床,例如铜和钼,以加强该地区的开采活动。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
MULTIFACETED INVESTIGATION OF PORPHYRY CU-AU-MO DEPOSIT IN HYDROTHERMAL ALTERATION ZONES WITHIN THE GOLD FIELD OF ILESHA SCHIST BELT
This study was carried out to map the distribution of porphyry systems within Ilesha Schist belt Southwestern Nigeria for easy accessibility of commercial gold as well as copper and molybdenum deposits to boost exploitation activities within the area. Airborne magnetic and radiometric data of the area were utilized. The acquired total magnetic intensity map of the field was enhanced with reduction to equator, vertical derivative, analytic signal and spectral analysis. Enhanced total magnetic intensity map of the study area revealed magnetic anomalies related to concealed intrusive rock associated with Cu-Au-Mo deposit at depth ranges from 306 – 421 m. Vertical derivative map revealed shallow magnetic bodies in the southern and western parts, which are probable zones for Cu-Au-Mo deposit. Analytical signal map, with magnetic zones of high intensity value between 0.1 nT/M and 1.7 nT/M highlighted faulted basement blocks impregnated with porphyry the Cu-Au-Mo deposit. Airborne radiometry image shows radioelement distributions for different lithologies. High concentration of potassium signatures observed over some parts of the area revealed hydrothermal alteration zones favourable to concentration of Cu-Au-Mo deposits. Computed Th/k ratio and composite potassium maps enhanced the signature of potassium enrichment associated with hydrothermal alteration zones. Validation of airborne results using geochemical analyses confirms the presence of copper-gold-molybdenum elements within the mapped hydrothermal alteration zones. This research has identified other valuable ore deposit, such as copper and molybdenum, to enhance exploitation activities within the area.
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