Mapping and discrimination of the mineralization potential in the Bonako area (Central Cameroon Domain): Insights from Landsat 9 OLI data, GIS fuzzy modeling techniques and field observations

Nguimezap Marie Madeleine , Fozing Eric Martial , Safianou Ousmanou , Achu Megnemo Ludovic , Sobze Yemdji Robinson Belmien , Sawadogo Sâga
{"title":"Mapping and discrimination of the mineralization potential in the Bonako area (Central Cameroon Domain): Insights from Landsat 9 OLI data, GIS fuzzy modeling techniques and field observations","authors":"Nguimezap Marie Madeleine ,&nbsp;Fozing Eric Martial ,&nbsp;Safianou Ousmanou ,&nbsp;Achu Megnemo Ludovic ,&nbsp;Sobze Yemdji Robinson Belmien ,&nbsp;Sawadogo Sâga","doi":"10.1016/j.geogeo.2024.100347","DOIUrl":null,"url":null,"abstract":"<div><div>The Bonako area is situated in the Central Cameroon Domain of the Central African Fold Belt. In this study, the discrimination of lithological units with hydrothermally altered deposits is investigated by combining Landsat 9 OLI data, fieldwork descriptions, GIS fuzzy modeling techniques, and remote sensing approaches including false color composite (FCC), de-correlation stretch (DS), standard principal component analysis (PCA) and minimum noise fraction (MNF). In addition, image processing methods such as band ratios (BR) and selective principal component analysis (Crosta-PCA) were applied to target and delineate hydrothermally altered and corresponding minerals and the spectral angle mapper (SAM) classification algorithm was used to classify the discriminated lithological units within the study area. The evaluation of the fuzzy membership of each alteration-derived mineral from Landsat 9 OLI and ASTER data indicates that the highest favourability index varies from 0.8 to 1 indicating a rating index related to iron mineralization. The integration of selected remote sensing methods allowed the identification of gabbro, granites, gneiss, and mylonites with iron-oxides, hydroxyl/clay, and ferrous occurrences as potential mineralization in the Bonako area. The analysis of lineaments illustrated two main structural trends (N-S and NE-SW) and an accessory one (E-W) in the study area. Merging these with the identified formations highlighted the formations with mineral deposits. Subsequently, the lithological maps displaying alteration minerals and lineaments were validated by fieldwork investigations and microscopic data. Quantitatively, the overall accuracy of the SAM method is 100 %, which also validates the effectiveness of the classification of lithologies using Landsat 9 OLI data. This research predicts how the integration and processing of Landsat 9 OLI, Fuzzy, ASTER data, and field investigations can simplify the identification of rock units with potentially mineralized zone. It also suggests that such a combined method is useful in defining targeted mineralized areas during exploration research.</div></div>","PeriodicalId":100582,"journal":{"name":"Geosystems and Geoenvironment","volume":"4 1","pages":"Article 100347"},"PeriodicalIF":0.0000,"publicationDate":"2025-02-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Geosystems and Geoenvironment","FirstCategoryId":"1085","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S2772883824000979","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 0

Abstract

The Bonako area is situated in the Central Cameroon Domain of the Central African Fold Belt. In this study, the discrimination of lithological units with hydrothermally altered deposits is investigated by combining Landsat 9 OLI data, fieldwork descriptions, GIS fuzzy modeling techniques, and remote sensing approaches including false color composite (FCC), de-correlation stretch (DS), standard principal component analysis (PCA) and minimum noise fraction (MNF). In addition, image processing methods such as band ratios (BR) and selective principal component analysis (Crosta-PCA) were applied to target and delineate hydrothermally altered and corresponding minerals and the spectral angle mapper (SAM) classification algorithm was used to classify the discriminated lithological units within the study area. The evaluation of the fuzzy membership of each alteration-derived mineral from Landsat 9 OLI and ASTER data indicates that the highest favourability index varies from 0.8 to 1 indicating a rating index related to iron mineralization. The integration of selected remote sensing methods allowed the identification of gabbro, granites, gneiss, and mylonites with iron-oxides, hydroxyl/clay, and ferrous occurrences as potential mineralization in the Bonako area. The analysis of lineaments illustrated two main structural trends (N-S and NE-SW) and an accessory one (E-W) in the study area. Merging these with the identified formations highlighted the formations with mineral deposits. Subsequently, the lithological maps displaying alteration minerals and lineaments were validated by fieldwork investigations and microscopic data. Quantitatively, the overall accuracy of the SAM method is 100 %, which also validates the effectiveness of the classification of lithologies using Landsat 9 OLI data. This research predicts how the integration and processing of Landsat 9 OLI, Fuzzy, ASTER data, and field investigations can simplify the identification of rock units with potentially mineralized zone. It also suggests that such a combined method is useful in defining targeted mineralized areas during exploration research.

Abstract Image

Bonako地区(喀麦隆中部地区)成矿潜力的制图与识别:来自Landsat 9 OLI数据、GIS模糊建模技术和野外观测的见解
博纳科地区位于中非褶皱带的喀麦隆中部地区。本研究结合Landsat 9 OLI数据、野外工作描述、GIS模糊建模技术以及假色合成(FCC)、去相关拉伸(DS)、标准主成分分析(PCA)和最小噪声分数(MNF)等遥感方法,研究了热液蚀变沉积岩性单元的识别。利用波段比(BR)和选择性主成分分析(Crosta-PCA)等图像处理方法对研究区内热液蚀变物及其对应矿物进行了定位圈定,并利用光谱角映射器(SAM)分类算法对已识别的岩性单元进行了分类。利用Landsat 9 OLI和ASTER资料对各蚀变矿物进行模糊隶属度评价,结果表明,最高有利度指数在0.8 ~ 1之间,为与铁成矿有关的分级指标。选定的遥感方法的整合允许识别辉长岩、花岗岩、片麻岩和糜伦岩与氧化铁、羟基/粘土和铁矿床在Bonako地区作为潜在的矿化。地形特征分析表明,研究区有两个主要的构造走向(N-S和NE-SW)和一个辅助的构造走向(E-W)。将这些与已识别的地层合并,突出显示了含有矿床的地层。随后,通过野外调查和显微资料验证了显示蚀变矿物和地貌的岩性图。定量地说,SAM方法的总体精度为100%,这也验证了使用Landsat 9 OLI数据进行岩性分类的有效性。本研究预测了Landsat 9 OLI、Fuzzy、ASTER数据的整合和处理以及野外调查如何简化具有潜在矿化带的岩石单元的识别。同时也说明了这种组合方法在勘探研究中对于确定目标矿化区是有用的。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
求助全文
约1分钟内获得全文 求助全文
来源期刊
CiteScore
4.70
自引率
0.00%
发文量
0
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
确定
请完成安全验证×
copy
已复制链接
快去分享给好友吧!
我知道了
右上角分享
点击右上角分享
0
联系我们:info@booksci.cn Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。 Copyright © 2023 布克学术 All rights reserved.
京ICP备2023020795号-1
ghs 京公网安备 11010802042870号
Book学术文献互助
Book学术文献互助群
群 号:481959085
Book学术官方微信