铁矿床的高分辨率航空磁探测

Fahad Abubakar , Ismail Ahmad Abir
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引用次数: 0

摘要

钢铁工业一直被称为工业化的“支柱”和国民经济的“基石”。近50年来,尼日利亚一直在努力在尼日利亚的铁矿石中心科吉州建设一个公共资助的钢铁行业,以加快该国的经济发展。然而,阻碍这一努力的最重要的地球科学障碍是当地材料的不可预测性,特别是铁矿石,以及探索更多材料的崎岖地形挑战。为了缓解这一挑战,尼日利亚地质调查局进行了高分辨率航空磁测量。本研究旨在利用最近获得的高分辨率航空磁数据集描绘Kogi州铁矿石资源的空间产状。以已知铁矿为对照,采用CET (Centre for Exploration Targeting)网格分析、解析信号和欧拉反褶积分析技术辅助解释。总磁强图和残差图不能通过单纯的定性解释揭示潜在矿床。由于研究区地质构造的复杂性,线体密度图与已知铁矿床的一致性很差。然而,分析信号图的高振幅峰值是一致的,与所有已知的现有矿山完全相关,并揭示了潜在的铁矿床。峰值范围为0.147 ~ 0.430 nT/m。Euler反褶积显示潜在矿床深度为250 m,解析信号显示深度范围为49.594 ~ 150.926 m。与以往的相关研究相比,分析信号的深度估计更浅,振幅峰值相对较高。这些都归功于本研究的高分辨率采集参数。最后,我们建议利益相关者和决策者优先考虑分析信号的高振幅峰值作为进一步铁矿石勘探和开采过程的目标区域。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

High-resolution airborne magnetic detection of iron ore deposits

High-resolution airborne magnetic detection of iron ore deposits
The iron and steel industry has been called the "backbone" of industrialisation and the "bedrock" of national economies. For almost 50 years, Nigeria has endeavoured to construct a publicly sponsored iron and steel sector in Kogi State, Nigeria's iron ore hub, to expedite the nation's economic development. However, amongst the most significant geoscientific barriers hindering this endeavour are the unpredictability of local materials, notably iron ores, and the rugged topographical challenge of exploring more materials. As a part of the process of abating this challenge, a high-resolution airborne magnetic survey was conducted by the Nigerian Geological Survey Agency. This study aims to delineate the spatial occurrences of the iron ore resources in Kogi State using the recently acquired high-resolution airborne magnetic datasets. The Centre for Exploration Targeting (CET) grid analysis, analytic signal, and Euler deconvolution analytical technique were employed to aid the interpretation, and the known iron ore mines were used as control. The total magnetic intensity and residual map did not reveal the potential ore deposits by mere qualitative interpretation. The lineament density map displays a very poor consistency with the known iron ore deposits due to the geostructural complexity of the study area. However, the high-amplitude peaks of the analytic signal map are consistent, perfectly correlate with all the known existing mines, and reveal potential iron ore deposits. These peaks are in the range of 0.147 to 0.430 nT/m. The Euler deconvolution reveals the depth of potential deposits to be <250 m, while the analytic signal reveals a depth range of 49.594 to 150.926 m. Compared with previous related studies, shallower depth estimates and relatively higher amplitude peaks from the analytic signal were observed. These were attributed to this study's higher resolution acquisition parameters. Finally, we recommend that stakeholders and policymakers prioritize the high-amplitude peaks of the analytic signal as target zones for further iron ore exploration and exploitation processes.
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