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尼日利亚西北部凯比州南部及其周边地区金矿成矿潜力的综合地球物理勘查

Integrated geophysical Investigation for gold mineralization potential over southern parts of Kebbi state and its Environs, northwestern Nigeria.

作者信息

Salako K A, Adetona A A, Rafiu A A, Augie A I, Jimoh M O, Alkali A, Muriana R A, Lawrence J O

机构信息

Department of Geophysics, Federal University of Technology Minna, Nigeria.

Department of Applied Geophysics, Federal University Birnin Kebbi, Nigeria.

出版信息

Heliyon. 2024 Jul 4;10(14):e34093. doi: 10.1016/j.heliyon.2024.e34093. eCollection 2024 Jul 30.

Abstract

The potential zones of gold mineralization were identified in this study using aeromagnetic and aero-radiometric methods. The Nigerian Geological Survey Agency (NGSA) provided half-degree airborne magnetic and radiometric datasets covering the southern part of Kebbi State. Magnetic data were subjected to first vertical derivative (1VD), total gradient amplitude (TGA), total horizontal derivative (THD), source edge detection (SED), center for exploration targeting (CET), Euler deconvolution (ED) and source parameter imaging (SPI) to identify favourable structures to gold mineralization. Aero-radiometric data delineation of the region of hydrothermal alteration zones through the K/eTh ratio, K_deviation, F_parameters, and Ternary image analyses were successful. The results of the magnetic data techniques revealed the regions of major structures/or lineaments with gold mineralization attributes, trending in the NE to SW directions and the SE to NE parts of the study area. The depth to the structures of the magnetic source hosting gold mineralization was less than 5 m using algorithm ED and SPI techniques. Normalized radiometric data showed the area of anomalously high and moderate hydrothermal altered zones. The region's designation as a gold field is supported by major fault lines observed on the 1VD, a sequence of bristle fractures from the CET analysis, and high values of K_deviation and F_parameter, all of which are were visible on the Ternary images. The integrated results revealed zones of major structures and hydrothermal regions of gold fields at Agwara, Western Magama, Rijau, Fakai, Bukkuyum, and Borgu in the SE of the study area.

摘要

本研究采用航磁和航空放射性测量方法确定了金矿化的潜在区域。尼日利亚地质调查局(NGSA)提供了覆盖凯比州南部的半度航空磁测和放射性测量数据集。对磁数据进行了一阶垂直导数(1VD)、总梯度幅值(TGA)、总水平导数(THD)、源边缘检测(SED)、勘探目标中心(CET)、欧拉反褶积(ED)和源参数成像(SPI)处理,以识别有利于金矿化的构造。通过K/eTh比值、K偏差、F参数和三元图像分析,成功地对航空放射性数据进行了热液蚀变带区域的 delineation(此处原文有误,可能是“delimitation”,意为“划定”)。磁数据技术的结果揭示了具有金矿化属性的主要构造/线性构造区域,其走向为东北至西南方向以及研究区域的东南至东北部分。使用算法ED和SPI技术,承载金矿化的磁源构造深度小于5米。归一化放射性数据显示了异常高和中等热液蚀变带的区域。该区域被指定为金矿区得到了1VD上观察到的主要断层线、CET分析中的一系列刷毛状裂缝以及K偏差和F参数的高值的支持,所有这些在三元图像上都可见。综合结果揭示了研究区域东南部阿瓜拉、西马加马、里焦、法凯、布库尤姆和博尔古的主要构造带和金矿区的热液区域。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/a2a1/11292261/7fcddc461b0d/gr1.jpg

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