Implementing Digital Edge Enhancers on Improved High-Resolution Aeromagnetic Signals for Structural-Depth Analysis around the Middle Benue Trough, Nigeria

Digital edge detector operations using magnetic derivatives in conjunction with spectra depth analysis were performed on high-resolution aeromagnetic signals to enhance the delineation and interpretation of depth, structural, and intrasedimentary features within the Middle Benue Trough (MBT) of Nort...

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Autores principales: Eko Gerald Ejiga, Noer El Hidayah Ismail, Ismail Yusoff
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Publicado: MDPI AG 2021
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Acceso en línea:https://doaj.org/article/c5fb3ccee6f0409389ee362ec49f67fc
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spelling oai:doaj.org-article:c5fb3ccee6f0409389ee362ec49f67fc2021-11-25T18:26:35ZImplementing Digital Edge Enhancers on Improved High-Resolution Aeromagnetic Signals for Structural-Depth Analysis around the Middle Benue Trough, Nigeria10.3390/min111112472075-163Xhttps://doaj.org/article/c5fb3ccee6f0409389ee362ec49f67fc2021-11-01T00:00:00Zhttps://www.mdpi.com/2075-163X/11/11/1247https://doaj.org/toc/2075-163XDigital edge detector operations using magnetic derivatives in conjunction with spectra depth analysis were performed on high-resolution aeromagnetic signals to enhance the delineation and interpretation of depth, structural, and intrasedimentary features within the Middle Benue Trough (MBT) of North Central Nigeria, which could serve as a guide for mineral exploration. The derivatives revealed high-amplitude and short-wavelength anomalies over areas underlain by crystalline basement complexes, major volcanic zones, and aggregates of intrasedimentary volcanic and plutonic rocks. Geologic lineaments trending predominantly NE–SW and NW–SE, as well as minor trends of E–W and N–S, suggest that the area has undergone differential stress regimes across geologic time. The spectral depth analysis indicates a two-source depth model. The deep depth ranges from 1.9 to 6.1 km with an average of 3.9 km, whereas the shallow depth ranges between 0.3 and 1.9 km with an average of 0.8 km and is found to emanate from magnetic signals of post-Cretaceous near-surface igneous intrusions as well as other magnetized bodies embedded within the sediments. The spatial distribution of various hydrothermal minerals such as lead–zinc–barite deposits, as well as salt mineralization, is associated with the widespread Tertiary–recent magmatism and governed by pre-existing tectonic structures in the region.Eko Gerald EjigaNoer El Hidayah IsmailIsmail YusoffMDPI AGarticlemagnetic derivativespectral depth analysisMiddle Benue Troughintrusivehydrothermal mineralsedge detectorMineralogyQE351-399.2ENMinerals, Vol 11, Iss 1247, p 1247 (2021)
institution DOAJ
collection DOAJ
language EN
topic magnetic derivative
spectral depth analysis
Middle Benue Trough
intrusive
hydrothermal minerals
edge detector
Mineralogy
QE351-399.2
spellingShingle magnetic derivative
spectral depth analysis
Middle Benue Trough
intrusive
hydrothermal minerals
edge detector
Mineralogy
QE351-399.2
Eko Gerald Ejiga
Noer El Hidayah Ismail
Ismail Yusoff
Implementing Digital Edge Enhancers on Improved High-Resolution Aeromagnetic Signals for Structural-Depth Analysis around the Middle Benue Trough, Nigeria
description Digital edge detector operations using magnetic derivatives in conjunction with spectra depth analysis were performed on high-resolution aeromagnetic signals to enhance the delineation and interpretation of depth, structural, and intrasedimentary features within the Middle Benue Trough (MBT) of North Central Nigeria, which could serve as a guide for mineral exploration. The derivatives revealed high-amplitude and short-wavelength anomalies over areas underlain by crystalline basement complexes, major volcanic zones, and aggregates of intrasedimentary volcanic and plutonic rocks. Geologic lineaments trending predominantly NE–SW and NW–SE, as well as minor trends of E–W and N–S, suggest that the area has undergone differential stress regimes across geologic time. The spectral depth analysis indicates a two-source depth model. The deep depth ranges from 1.9 to 6.1 km with an average of 3.9 km, whereas the shallow depth ranges between 0.3 and 1.9 km with an average of 0.8 km and is found to emanate from magnetic signals of post-Cretaceous near-surface igneous intrusions as well as other magnetized bodies embedded within the sediments. The spatial distribution of various hydrothermal minerals such as lead–zinc–barite deposits, as well as salt mineralization, is associated with the widespread Tertiary–recent magmatism and governed by pre-existing tectonic structures in the region.
format article
author Eko Gerald Ejiga
Noer El Hidayah Ismail
Ismail Yusoff
author_facet Eko Gerald Ejiga
Noer El Hidayah Ismail
Ismail Yusoff
author_sort Eko Gerald Ejiga
title Implementing Digital Edge Enhancers on Improved High-Resolution Aeromagnetic Signals for Structural-Depth Analysis around the Middle Benue Trough, Nigeria
title_short Implementing Digital Edge Enhancers on Improved High-Resolution Aeromagnetic Signals for Structural-Depth Analysis around the Middle Benue Trough, Nigeria
title_full Implementing Digital Edge Enhancers on Improved High-Resolution Aeromagnetic Signals for Structural-Depth Analysis around the Middle Benue Trough, Nigeria
title_fullStr Implementing Digital Edge Enhancers on Improved High-Resolution Aeromagnetic Signals for Structural-Depth Analysis around the Middle Benue Trough, Nigeria
title_full_unstemmed Implementing Digital Edge Enhancers on Improved High-Resolution Aeromagnetic Signals for Structural-Depth Analysis around the Middle Benue Trough, Nigeria
title_sort implementing digital edge enhancers on improved high-resolution aeromagnetic signals for structural-depth analysis around the middle benue trough, nigeria
publisher MDPI AG
publishDate 2021
url https://doaj.org/article/c5fb3ccee6f0409389ee362ec49f67fc
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