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Lithological discrimination based on Landsat-9 OLI sensor and field observation data: The bana an-orogenic volcano-plutonic ring complex, West Cameroon line.

作者信息

Mohamed Rachid, Tamen Jules, Ousmanou Safianou, Yangouo Fadimatou Kimoun, Nkouathio David

机构信息

Department of Earth Science, University of Dschang, Dschang, Cameroon.

Department of Geological Research, CONGEO-Engineering, Yaounde, Cameroon.

出版信息

Heliyon. 2024 Aug 24;10(17):e36806. doi: 10.1016/j.heliyon.2024.e36806. eCollection 2024 Sep 15.

DOI:10.1016/j.heliyon.2024.e36806
PMID:39263140
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC11388743/
Abstract

The western region, encompassing the an-orogenic Bana volcano-plutonic ring complex in Cameroon, underwent comprehensive exploration involving remote sensing analysis, fieldwork investigations, petrographic, and volcanological studies. The primary objective of this work was to integrate remote sensing analysis, fieldwork, and laboratory studies to achieve accurate lithological mapping for future prospective mineral explorations in the study area. Field relationships among co-occurring rock units in the area were examined, utilizing Landsat-9 OLI data. Petrographic analysis, including the use of a polarizing microscope, was conducted on various rock units (15 samples), along with volcanological processes studies. Operational Land Imager (OLI) images of Landsat 9 were processed using algorithms including False Colour Composite (FCC), Decorrelation Stretch (DS), Band Ratio (BR) composite, Principal Component Analysis (PCA), Spectral Angle Mapper (SAM) and Constrained Energy Minimization (CEM) methods to identify distinct rock units in the Bana ring complex. As a result, the later methods permitted to identify the petrographic units of the ring complex, which primarily comprise a volcano-plutonic sequence, along with metamorphic rocks like gneisses. The volcanic units include variety of basalts, trachytes, rhyolites and volcanic tuffs, while the plutonic units including gabbros, diorites, syenites and fine-grained granites. The findings of this study accurately at 99 % have permitted to newly setup a geologic map of the study area with implications for future mineral explorations.

摘要
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/54a2/11388743/e848e5660797/gr16.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/54a2/11388743/d1a85dc8faec/gr1.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/54a2/11388743/17c14d5f085c/gr2.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/54a2/11388743/9787077a14f4/gr3.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/54a2/11388743/54de0b83c163/gr4.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/54a2/11388743/9750c6d8ab88/gr5.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/54a2/11388743/8b0e744d2721/gr6.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/54a2/11388743/ce08a361143c/gr7.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/54a2/11388743/bdbc33bacfe9/gr8.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/54a2/11388743/9853274ff086/gr9.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/54a2/11388743/0e48b8f00243/gr10.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/54a2/11388743/6e3e36072c27/gr11.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/54a2/11388743/de5483b3e0bf/gr12.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/54a2/11388743/51236cc46690/gr13.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/54a2/11388743/865d434d6f18/gr14.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/54a2/11388743/6a28c7f07c8e/gr15.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/54a2/11388743/e848e5660797/gr16.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/54a2/11388743/d1a85dc8faec/gr1.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/54a2/11388743/17c14d5f085c/gr2.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/54a2/11388743/9787077a14f4/gr3.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/54a2/11388743/54de0b83c163/gr4.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/54a2/11388743/9750c6d8ab88/gr5.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/54a2/11388743/8b0e744d2721/gr6.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/54a2/11388743/ce08a361143c/gr7.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/54a2/11388743/bdbc33bacfe9/gr8.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/54a2/11388743/9853274ff086/gr9.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/54a2/11388743/0e48b8f00243/gr10.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/54a2/11388743/6e3e36072c27/gr11.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/54a2/11388743/de5483b3e0bf/gr12.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/54a2/11388743/51236cc46690/gr13.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/54a2/11388743/865d434d6f18/gr14.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/54a2/11388743/6a28c7f07c8e/gr15.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/54a2/11388743/e848e5660797/gr16.jpg

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本文引用的文献

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Heliyon. 2023 Dec 6;10(1):e23334. doi: 10.1016/j.heliyon.2023.e23334. eCollection 2024 Jan 15.