使用地球化学、地磁、诱导极化和电阻率方法划分尼日利亚中北部库沙卡片岩带潜在金矿化区

IF 1.5 4区 工程技术 Q3 METALLURGY & METALLURGICAL ENGINEERING
Sherif Olumide Sanusi, Deborah Ima-Abasi Josiah, Oladele Olaniyan, Gbenga Moses Olayanju
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引用次数: 0

摘要

这项研究将地球物理方法(地面磁学、电阻率和感应极化测量)与火法化验和电感耦合等离子体-原子发射光谱技术相结合,在库沙卡绿岩带划定了造山金矿潜在区。对磁性数据采用了不同的边缘检测滤波器和三维欧拉解卷积技术,以划定控制研究区域造山金矿化的地质结构。VOXI Earth Modeling™ 软件应用于感应极化和电阻率数据,以生成研究区域的金矿化目标。根据本研究的地球化学发现,该矿带的成因金矿化与方铅矿、闪锌矿、独居石、韧皮石和氧化锰矿物有关,并具有变质成因。全磁场结果表明,NE-SW 和 NW-SE 走向结构主要与金化验热点有关,表明该带的造山金矿与泛非造山事件有关。带有散生硫化金矿床和热液蚀变晕的断裂带表现出低电阻率和高电荷率特征。然而,在强烈硅化的变质岩中出现的浸润石英脉和断裂带的散生硫化金矿床则表现出高电荷率和高电阻率特征。生成的金矿化靶标模型与地质构造、元古代岩石和金热点有很好的相关性,表明岩性和地质构造优先控制着该带的成因金矿化。因此,本研究收集的信息将有助于采矿者和学术界确定该地区未来金勘探项目的钻孔位置。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Delineation of Potential Gold Mineralization Zones in the Kushaka Schist Belt, Northcentral Nigeria, Using Geochemical, Ground Magnetic, Induced Polarization, and Electrical Resistivity Methods

Delineation of Potential Gold Mineralization Zones in the Kushaka Schist Belt, Northcentral Nigeria, Using Geochemical, Ground Magnetic, Induced Polarization, and Electrical Resistivity Methods

This study integrated geophysical methods (ground magnetics, electrical resistivity, and induced polarization measurements) in conjunction with fire assay and inductively coupled plasma-atomic emission spectrometry techniques to delineate orogenic gold mineralization potential zones in the Kushaka greenschist belt. Different edge detection filters and a 3D Euler deconvolution technique were applied to magnetic data to delineate geologic structures that control orogenic gold mineralization in the study area. VOXI Earth Modeling™ software was applied to induced polarization and electrical resistivity data to generate gold mineralized targets in the study area. Based on the geochemical findings in this study, orogenic gold mineralization in the belt is associated with galena, sphalerite, monazite, bastnaesite, and manganese oxide minerals and has a metamorphic origin. The total magnetic field results indicate that NE-SW and NW–SE trending structures are primarily associated with gold assay hotspots, indicating that orogenic gold mineralization in this belt is connected to Pan-African orogenic events. Fractured zones with disseminated gold-sulfide deposits and hydrothermal alteration halos exhibit low resistivity and high chargeability signatures. However, the occurrence of disseminated gold-sulfide deposits that infilled quartz veins and fractured zones in the intensely silicified metasedimentary rocks exhibit high chargeability and high resistivity signatures. The produced gold mineralized targeting model correlates well with geologic structures, metasedimentary rocks, and gold hotspots, indicating that lithologies and geologic structures preferentially control orogenic gold mineralization in the belt. Hence, the information gathered in this study would assist miners and academia in determining the drill-hole locations for future gold exploration programs in the area.

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来源期刊
Mining, Metallurgy & Exploration
Mining, Metallurgy & Exploration Materials Science-Materials Chemistry
CiteScore
3.50
自引率
10.50%
发文量
177
期刊介绍: The aim of this international peer-reviewed journal of the Society for Mining, Metallurgy & Exploration (SME) is to provide a broad-based forum for the exchange of real-world and theoretical knowledge from academia, government and industry that is pertinent to mining, mineral/metallurgical processing, exploration and other fields served by the Society. The journal publishes high-quality original research publications, in-depth special review articles, reviews of state-of-the-art and innovative technologies and industry methodologies, communications of work of topical and emerging interest, and other works that enhance understanding on both the fundamental and practical levels.
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