Integrated aeromagnetic and airborne radiometric analysis for structural mapping and mineralisation potential in the Naraguta Area, North-Central Nigeria

Mubarak Umar Faruk, Solomon Nehemiah Yusuf, Raymond Ishaya Daspan
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Abstract

This research provides insights into the structural settings and geochemically altered zones within Naraguta and its environs. Various enhancement techniques were employed to identify the edges of structures controlling the magnetic field direction, the location, and the morphology of causative bodies. Source parameter imaging was used to analyse the depth of magnetic sources. Radiometric data processing was performed to identify alteration zones. Maps such as the K/Th and K/U, as well as the U/Th and U/K ratio maps, and a normalised ternary map were generated. From the magnetic analysis. Intrusions such as the Neil's Valley granite porphyry and Naraguta quartz pyroxene-fayalite-porphyry were delineated, along with rhyolites and pyroclastics. The study area’s structures predominantly trend northeast-southwest, with additional orientations reflecting Pan-African orogeny structures, which may be linked to hydrothermal deposits. In addition, these could be related to different geological processes, such as faulting, jointing, or regional stress patterns. They can lead to structural alignments even in non-orogenic environments like the Younger Granites. The K/Th ratio values of 0.20 % ppm−1were identified above the expected background in an acidic environment, implying possible mineralisation such as tin and its associates as well as rare earths. Geochemical alteration zones were present in various parts of the area in alignment with magnetic lines, implying mineralisation potential.
尼日利亚中北部Naraguta地区构造测绘和矿化潜力的综合航空磁和航空辐射分析
这项研究提供了对Naraguta及其周边地区的构造环境和地球化学蚀变带的见解。利用各种增强技术来识别控制磁场方向、位置和致病体形态的结构边缘。利用磁源参数成像技术对磁源深度进行分析。进行了辐射数据处理,以确定蚀变带。生成了K/Th和K/U等映射,以及U/Th和U/K比率映射和规范化三元映射。从磁性分析。圈定了尼尔谷花岗斑岩、Naraguta石英辉石-绢长斑岩、流纹岩和火山碎屑等侵入体。研究区构造以东北—西南方向为主,另有泛非洲造山构造,可能与热液矿床有关。此外,这些可能与不同的地质作用有关,如断层、节理或区域应力模式。它们甚至可以在像新花岗岩这样的非造山环境中导致构造排列。在酸性环境中,K/Th比值值为0.20 % ppm−1,高于预期的背景值,这意味着可能存在矿化,如锡及其伴生物以及稀土。该区多处地球化学蚀变带与磁力线排列一致,具有成矿潜力。
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