Depth estimation of the residualfield of Patigi Area, Nigeria , using source parameter imaging and spectral depth analysis

Aeromagnetic depth estimation was carried out over a one-half-degree sheet in the southwestern Bida Basin, Northcentral Nigeria. The area, bounded by latitudes 8◦30′–9◦0′ N and longitudes 5◦30′–6◦0′ E, is underlain by Campanian–Maastrichtian sandstones and basement rocks of granite-gneiss and migmat...

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Main Authors: S. A. Salaudeen, T. A. Adagunodo, A. O. Busari, K. O. Suleman, L. A. Sunmonu
Format: Article
Language:English
Published: FLAYOO PUBLISHING HOUSE LIMITED 2025-07-01
Series:Recent Advances in Natural Sciences
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Online Access:https://flayoophl.com/journals/index.php/rans/article/view/210
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author S. A. Salaudeen
T. A. Adagunodo
A. O. Busari
K. O. Suleman
L. A. Sunmonu
author_facet S. A. Salaudeen
T. A. Adagunodo
A. O. Busari
K. O. Suleman
L. A. Sunmonu
author_sort S. A. Salaudeen
collection DOAJ
description Aeromagnetic depth estimation was carried out over a one-half-degree sheet in the southwestern Bida Basin, Northcentral Nigeria. The area, bounded by latitudes 8◦30′–9◦0′ N and longitudes 5◦30′–6◦0′ E, is underlain by Campanian–Maastrichtian sandstones and basement rocks of granite-gneiss and migmatites. Potential field methods were applied to investigate subsurface sedimentary thickness. Regional–residual separation was achieved using polynomial fitting, and the residual field was analyzed using source parameter imaging (SPI) and power spectrum techniques for depth estimation around Pategi and environs. The residual map was subdivided into nine spectral sections to examine depth variations from magnetic sources. SPI results revealed depths ranging from 53.4m to 2766.5m, with a mean of 284.3m. Spectral analysis indicated shallow magnetic sources between 0.730km to 1.359km (average 1.100km) and deeper sources between 1.927km to 2.840km (average 2.333km). The maximum sedimentary thickness of 2.840km was found in the north-central area, including Pategi, Baradogi, Wando, and Edogi. These results indicate significant hydrocarbon potential. Integrated geological and geophysical studies are recommended to validate reservoir structures and assess viability for exploration.
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institution Kabale University
issn 1596-0544
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language English
publishDate 2025-07-01
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spelling doaj-art-0e93b55beb7e49bea1fef27eec01733f2025-08-20T03:56:42ZengFLAYOO PUBLISHING HOUSE LIMITEDRecent Advances in Natural Sciences1596-05441596-07572025-07-013210.61298/rans.2025.3.2.210Depth estimation of the residualfield of Patigi Area, Nigeria , using source parameter imaging and spectral depth analysisS. A. SalaudeenT. A. AdagunodoA. O. BusariK. O. SulemanL. A. SunmonuAeromagnetic depth estimation was carried out over a one-half-degree sheet in the southwestern Bida Basin, Northcentral Nigeria. The area, bounded by latitudes 8◦30′–9◦0′ N and longitudes 5◦30′–6◦0′ E, is underlain by Campanian–Maastrichtian sandstones and basement rocks of granite-gneiss and migmatites. Potential field methods were applied to investigate subsurface sedimentary thickness. Regional–residual separation was achieved using polynomial fitting, and the residual field was analyzed using source parameter imaging (SPI) and power spectrum techniques for depth estimation around Pategi and environs. The residual map was subdivided into nine spectral sections to examine depth variations from magnetic sources. SPI results revealed depths ranging from 53.4m to 2766.5m, with a mean of 284.3m. Spectral analysis indicated shallow magnetic sources between 0.730km to 1.359km (average 1.100km) and deeper sources between 1.927km to 2.840km (average 2.333km). The maximum sedimentary thickness of 2.840km was found in the north-central area, including Pategi, Baradogi, Wando, and Edogi. These results indicate significant hydrocarbon potential. Integrated geological and geophysical studies are recommended to validate reservoir structures and assess viability for exploration. https://flayoophl.com/journals/index.php/rans/article/view/210Aeromagnetic interpretationSpectral depthSource parameter imagingSedimentary thicknessBida Basin
spellingShingle S. A. Salaudeen
T. A. Adagunodo
A. O. Busari
K. O. Suleman
L. A. Sunmonu
Depth estimation of the residualfield of Patigi Area, Nigeria , using source parameter imaging and spectral depth analysis
Recent Advances in Natural Sciences
Aeromagnetic interpretation
Spectral depth
Source parameter imaging
Sedimentary thickness
Bida Basin
title Depth estimation of the residualfield of Patigi Area, Nigeria , using source parameter imaging and spectral depth analysis
title_full Depth estimation of the residualfield of Patigi Area, Nigeria , using source parameter imaging and spectral depth analysis
title_fullStr Depth estimation of the residualfield of Patigi Area, Nigeria , using source parameter imaging and spectral depth analysis
title_full_unstemmed Depth estimation of the residualfield of Patigi Area, Nigeria , using source parameter imaging and spectral depth analysis
title_short Depth estimation of the residualfield of Patigi Area, Nigeria , using source parameter imaging and spectral depth analysis
title_sort depth estimation of the residualfield of patigi area nigeria using source parameter imaging and spectral depth analysis
topic Aeromagnetic interpretation
Spectral depth
Source parameter imaging
Sedimentary thickness
Bida Basin
url https://flayoophl.com/journals/index.php/rans/article/view/210
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