Aeromagnetic delineation of iron ore deposits in a complex geological terrain aided by fuzzy logic

Fahad Abubakar, Felix Bamidele Fatoye, Momohjimoh Abdulsalami, Abdullateef Aliyu
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Abstract

The discovery of iron ore deposits is crucial for Nigeria’s economic diversification. However, the Nigerian Bida Basin’s complex geology, extensive overburden, disputed stratigraphic boundaries and limited surface exposure hinder traditional geological and geophysical exploration methods. This study employs high-resolution aeromagnetic data covering 20,984.48 m² to delineate subsurface geological features and identify potential mineralized zones. Known ore deposits were used for validation. Signal enhancement filters, including the analytic signal (ANS), total horizontal derivative (THD), and Euler deconvolution, were applied to aid data interpretation. Depth estimates for mineralization sources range from 83.06 to 248.53 m (ANS) and 129 to 600 m (Euler). The THD highlights magnetic edge sources, with gradient amplitudes of 0.00008–0.00046 nT/m, covering 4621.42 m² (22%). The ANS refines the geometric configuration of these zones, identifying high-amplitude regions (0.07–0.16 nT/m) across 2989.34 m² (14%). These results strongly align with existing mining sites. Fuzzy membership and fuzzy overlay spatial analysis integrated the geophysical results, identifying 2667.39 m² (12.7%) as highly suitable for future metallic ore exploration. Validation using four known iron ore mining sites confirmed model accuracy, with all sites located within predicted high-potential zones. The predicted high mineralization potential zones are focus areas for further exploration and development. While the findings demonstrate the effectiveness of integrated geophysical enhancements in complex terrains, future exploration should incorporate ground-truth validation and economic feasibility assessments to refine exploration accuracy and ensure resource viability.

Abstract Image

基于模糊逻辑的复杂地质地形下铁矿床航磁圈定
铁矿石储量的发现对尼日利亚的经济多样化至关重要。然而,尼日利亚Bida盆地复杂的地质、广泛的覆盖层、有争议的地层边界和有限的地表暴露,阻碍了传统的地质和地球物理勘探方法。利用20984.48 m²的高分辨率航磁数据,圈定地下地质特征,识别潜在矿化带。已知的矿床被用于验证。信号增强滤波器,包括分析信号(ANS)、总水平导数(THD)和欧拉反卷积,用于辅助数据解释。成矿源深度估计范围为83.06 ~ 248.53 m (ANS)和129 ~ 600 m (Euler)。THD突出磁边源,梯度幅值为0.00008 ~ 0.00046 nT/m,覆盖面积为4621.42 m²(22%)。ANS细化了这些区域的几何结构,确定了2989.34 m²(14%)的高振幅区域(0.07-0.16 nT/m)。这些结果与现有的采矿地点非常吻合。模糊隶属度和模糊叠加空间分析综合了物探结果,确定2667.39 m²(12.7%)为未来高度适合找矿的区域。使用四个已知的铁矿石开采地点进行验证,证实了模型的准确性,所有地点都位于预测的高潜力区域内。预测的高成矿潜力带是今后勘探开发的重点区域。虽然研究结果证明了综合地球物理增强在复杂地形中的有效性,但未来的勘探应结合地面真实性验证和经济可行性评估,以提高勘探精度并确保资源可行性。
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