Mapping geological configuration using geophysics data: an investigative approach in targeting iron ore, gold mineralization and other commodities, a case study of Toko-Nlokeng area (Nyong Greenstone Belt, SW Cameroon)

Pub Date : 2023-04-03 DOI:10.1080/25726838.2023.2218686
Yannick Saturnin Evina Aboula, Joseph Mvondo Ondoa, P. Ndjigui
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Abstract

ABSTRACT Regional geophysical data are important for detecting the presence of mineral deposits under cover. This study used geophysical data coupled with field geology of the Toko-Nlokeng area, Cameroon, to locate and map structures and lithologies as part of an exploration campaign for mineral deposits. The airborne geophysical survey in the Toko-Nlokeng area located in the Nyong complex revealed a predominantly EW striking highly folded series result of polyphase deformation of iron formations and host rocks divided into domains based on magnetic and radiometric character. The geophysical data indicate that major faults and shear zones strike NE-SW, with N–S striking units on the western margin and mainly E–W striking units in the rest of the area. These data suggest a major N–S thrust fault similar to the Borborema Province (NE Brazil) terrane marked by accretionary processes during the assembly of Western Gondwana. Several significant NE–SW striking shear zones are present. The data revealed many moderate to highly magnetic bodies that are interpreted as magnetite-bearing iron formation, mafic–ultramafic intrusions and flows, skarns, carbonatites and kimberlites. The magnetic and radiometric trends reveal the internal regional rock fabric and strike, and iron ore targets with magnetic anomaly up to 27,000 nT related to iron formations and other significant targets for gold, potassium (alteration) and uranium. The Toko-Nlokeng iron deposit is comprised of magnetite-bearing quartzite beds and is concordant with the surrounding host rocks and stands as one of a broad group of magnetite-dominated iron formations that occur throughout West and Central Africa. A new geological map was produced from mapped lithologies and microstructure characteristics of the iron formations, interpretations of the aeromagnetic data and structural features. The study results have important implications for regional exploration programs.
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利用地球物理数据绘制地质构造图:一种针对铁矿石、金矿化和其他商品的调查方法,以Toko-Nlokeng地区(喀麦隆西南部Nyong绿岩带)为例
区域地球物理数据对于探测被盖层下是否存在矿床具有重要意义。这项研究利用地球物理数据和喀麦隆东京-恩洛肯地区的野外地质资料,定位和绘制构造和岩性图,作为矿藏勘探活动的一部分。在位于Nyong杂岩的Toko-Nlokeng地区进行的航空地球物理调查显示,铁地层和主岩的多期变形以东西向为主,高度褶皱系,根据磁性和放射性特征划分了不同的域。地球物理资料表明,主要断裂和剪切带走向NE-SW,西缘以N-S走向为主,其余地区以E-W走向为主。这些资料表明,在西冈瓦纳拼合期间,存在一条与巴西东北部borborrema省(Borborema Province)类似的北向南逆冲大断层,标志着增生过程。存在几个重要的NE-SW走向剪切带。数据显示了许多中等至高磁性体,被解释为含磁铁矿的铁地层、基性-超基性侵入和流动、矽卡岩、碳酸盐岩和金伯利岩。磁性和放射性趋势揭示了区域内部的岩石结构和走向,以及与铁地层相关的磁异常高达27,000 nT的铁矿靶区和其他重要的金、钾(蚀变)和铀靶区。Toko-Nlokeng铁矿床由含磁铁矿石英岩床组成,与周围的寄主岩石一致,是整个西非和中非以磁铁矿为主的铁地层之一。根据铁地层的岩性和微观结构特征、航磁资料和构造特征的解释,绘制了新的地质图。研究结果对区域勘探规划具有重要意义。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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