Geospatial and Aeromagnetic investigation of structural lineaments in the Adamawa/Taraba region, upper Benue trough, NE Nigeria: An Implication for Geo-hazard occurrence

Authors

Keywords:

Structural lineaments, Geo-hazards, Aeromagnetic, Upper Benue Trough

Abstract

This study integrates geospatial and aeromagnetic techniques to delineate structural lineaments within the Adamawa-Taraba region of the Upper Benue Trough, northeastern Nigeria, stressing their implications for geo-hazard occurrence. Shuttle Radar Topography Mission (SRTM) Digital Elevation Model (DEM) was processed using GIS and High-resolution aeromagnetic data advanced filtering techniques including Reduction-to-Equator (RTE), First Vertical Derivative (FVD), Analytic Signal, Tilt Derivative (TDR), Horizontal Gradient Magnitude (HGM), and Source Parameter Imaging (SPI). The results reveal dominant structural trends oriented NE-SW and NW-SE, consistent with the regional tectonic framework of the Benue Trough. Lineament extraction and lineament density analysis indicate zones of intense fracturing, particularly in the central, southern, and northeastern parts of the study area, reflecting significant tectonic deformation. Depth estimates show variations from shallow depth of approximately 98 m to deep magnetic sources of depth of about 2200 m, corresponding to basement uplifts and sedimentary basins respectively. The spatial correlation between structural lineamentsand lineament density patterns highlights their strong control on geo-hazard distribution, including landslides, flooding, erosion, subsidence, and potential fault reactivation. The study demonstrates that integrated aeromagnetic and geospatial analysis provides an effective approach for delineating subsurface structures and identifying geo-hazard-prone zones, thereby supporting sustainable land-use planning and hazard mitigation strategies in structurally complex terrains.

Dimensions

Abdulsalam, N. N., Ogoh, E. K., & Ologe, O. (2022). Aeromagnetic investigation of subsurface structures in the Benue Trough, Nigeria.

Ahmed, Z. (2018). Geophysical interpretation of high‐resolution aeromagnetic data of part of southwestern Nigeria for subsurface mapping (Doctoral thesis). Ahmadu Bello University.

Ajakaiye, D. E., Hall, D. H., Ashiekaa, J. A., &Udensi, E. E. (1986). Aeromagnetic anomalies and tectonic trends in and around the Benue Trough, Nigeria.

Ajakaiye, D.E., (1986). Structures Deduced from Gravity data in the middle Benue Trough. Nigeria Journal of African Earth. 5, 359.

Bello, R., et al. (2022). Structural analysis of high-resolution aeromagnetic data over parts of Gongola Basin, NE Nigeria.

Benkhelil, J. (1989). The origin and evolution of the Cretaceous Benue Trough, Nigeria. Journal of African Earth Sciences, 8(2–4), 251–282.

Blakely, R.J. (1995). Potential Theory in Gravity and Magnetic Applications. Cambridge: Cambridge University Press.

Cooper, G.R.J., & Cowan, D.R. (2006). Enhancing potential field data using filters based on the local phase. Computers & Geosciences, 32(10), 1585–1591.

Dike, E.F.C. (1993). Stratigraphy and structure of the Gongola Basin, northeastern Nigeria: Implications for petroleum exploration. Journal of Mining and Geology, 29(2), 171–180.

Esri Inc. (2011). ArcGIS (Version 10.6). Esri Inc. https://www.esri.com/en-us/arcgis/products/ar

Fairhead, J. D., & Green, C. M. (1989). Controls on rifting and basin formation in Africa and South America. Tectonophysics, 163, 1–14

Grauch, V. J. S., Hudson, M. R., & Minor, S. A. (2009). Aeromagnetic expression of fault systems and mineralized belts in southern New Mexico and western Texas. Geosphere, 5(5), 598–621.

Ibraheem IM, Elawadi EA, El-Qady GM. (2018). Structural interpretation of aeromagnetic data for the Wadi El Natrun area, northwestern desert, Egypt. J Afr Earth Sci. 139:14–25. https://doi.org/10.1016/j.jafrearsci.2017.11.036.

Ijeh, I. B., et al. (2019). Integration of aeromagnetic and Landsat data for lineament mapping in Milligan PR, Gunn PJ. (1997). Enhancement and presentation of airborne geophysical data. AGSO J Aust GeolGeophys. 17(2):63–75

Li, X. (2006). Understanding 3D analytic signal amplitude. Geophysics, 71(2), L13–L16.

Ma, G., & Li, L. (2013). Alternative local wavenumber methods to estimate magnetic source parameters. Exploration Geophysics, 44(4), 264–271. https://doi.org/10.1071/EG13010

MacLeod, I.N., Jones, K., & Dai, T.F. (1993). 3-D analytic signal in the interpretation of total magnetic field data at low magnetic latitudes. Exploration Geophysics, 24(4), 679–688.

Milligan, P., & Gunn, P. (1997). Derivative filters in aeromagnetic data interpretation. Geophysics, 62(3), 904–915.

Miller HG, Singh V. 1994. Potential feld tilt-A new concept for location of potential feld sources. Journal of Applied Geophysics. 32(2–3):213–217. https://doi.org/10.1016/0926-9851(94)90022-1

Nabighian, M.N. (1972). The analytic signal of two-dimensional magnetic bodies with polygonal cross-section: Its properties and use for automated anomaly interpretation. Geophysics, 37(3), 507–517. https://doi.org/10.1190/1.1440276.

NASA Shuttle Radar Topography Mission (SRTM) (2013). Shuttle Radar Topography Mission (SRTM) Global. Distributed by OpenTopography. https://doi.org/10.5069/G9445JDF. Accessed 2026-04-10

Obaje, N.G. (2009). Geology and Mineral Resources of Nigeria. Berlin: Springer-Verlag.

Obaje, N.G., Wehner, H., Scheeder, G., Abubakar, M.B., &Jauro, A. (2006). Hydrocarbon prospectivity of Nigeria’s inland basins: From the viewpoint of organic geochemistry and organic petrology. AAPG Bulletin, 90(3), 325–353.

Olade, M. A. (1975). Evolution of Nigeria’s Benue Trough (aulacogen): A tectonic model. Geological Magazine, 112(6), 575–583.

Olatubosun, E. O., et al. (2022). Interpretation of aeromagnetic data for basement configuration in the Middle Benue Trough. Nigeria.

Opara, A. I., Onwuemesi, A. G., &Anudu, G. K. (2014). Analysis of aeromagnetic data over part of the Upper Benue Trough, northeastern Nigeria, using filters and source depth estimation techniques. Environmental Earth Sciences, 73, 7019–7032.

Oruç B, Keskinsezer A. (2008). Structural setting of the northeastern Biga Peninsula (Turkey) from tilt derivatives of gravity gradient tensors and magnitude of horizontal gravity components. Pure and Applied Geophysics. 165 (9–10):1913–1927. https://doi.org/10.1007/s00024-008-0407-8.

Petters, S.W. (1978). Stratigraphic evolution of the Benue Trough and its implications for the upper Cretaceous paleogeography of West Africa. Journal of Geology, 86(3), 311–322.

Phillips, J.D.(2000). Locating magnetic contacts: A comparison of the horizontal gradient, analytical signal and local wave number methods: 70th Annual International Meeting, SEG, Calgary Canada, Expanded Abstracts. 402-405.

Popoff, M. (1988). Du Gondwana à l’Atlantique Sud: Les connexions du fossé de la Benoué avec les bassins du Nord-Est brésilienjusqu’àl’ouverture du Golfe de Guinée. Bulletin des Centres de Recherches Exploration-Production Elf-Aquitaine, 12(1), 1–43.

Reid, A.B., Ebbing, J., & Webb, S.J. (2014). Avoidable Euler errors – the use and abuse of Euler deconvolution applied to potential fields. Geophysical Prospecting, 62(5), 1162–1168.

Roest, W.R., Verhoef, J., & Pilkington, M. (1992). Magnetic interpretation using the 3-D analytic signal. Geophysics, 57(1), 116–125. https://doi.org/10.1190/1.1443174.

Salem, A., Blakely, R. J., Green, C., Fairhead, J. D., & Ravat, D. (2014). Estimation of depth to top of magnetic sources using the local-wavenumber approach in an area of shallow Moho and Curie depth—The Red Sea. Geophysics.

Salem, A., Williams, S., Fairhead, J.D., Ravat, D., & Smith, R. (2007). Tilt-depth method: A simple depth estimation method using first-order derivatives of magnetic data. The Leading Edge, 26(12), 1502–1505.

Shahverdi M, Namaki L, Montahaei M, Mesbahi F, Basavand M. (2017). Interpretation of magnetic data based on Tilt derivative methods and enhancement of total horizontal gradient, a case study: zanjan Depression. J Earth Space Phys. 43(1):101–113.

Thurston, J.B, & Smith, R.S (1997). Automatic conversion of magnetic data to depth, dip, and susceptibility contrast using the SPI (TM) method. Geophysics 62:807–813. https://doi.org/10.1190/1.1444190

Ugwu, G. Z., & Alasi, T. K. (2016). Depth to magnetic sources and structural interpretation using aeromagnetic data in Nigeria.

Verduzco B, Fairhead .JD, Green, C.M, & MacKenzie C. (2004). New insights into magnetic derivatives for structural mapping. The Leading Edge. 23(2):116–119. https://doi.org/10.1190/1.1651454.

Waheed H. M, Mahmoud H. E & Mohamed Elsadek M. S (2023). Structural lineament analysis of the Bir El Qash area, Central Eastern Desert, Egypt, using integrated remote sensing and aeromagnetic data:Vol:.(1234567890) Scientifc Reports 13:21569 https://doi.org/10.1038/s41598-023-48660-x

Wright, J. B. (1968). South Atlantic continental drift and the Benue Trough. Nigeria.

Wright, J. B. (1981). Review of the origin and evolution of the Benue Trough in Nigeria. Earth-Science Reviews, 17(3), 239–249.

Published

2026-04-29

How to Cite

Sunu, S. A., Oniku, A. S., & Idi, B. Y. (2026). Geospatial and Aeromagnetic investigation of structural lineaments in the Adamawa/Taraba region, upper Benue trough, NE Nigeria: An Implication for Geo-hazard occurrence. Nigerian Journal of Physics, 35(2), 150-167. https://doi.org/10.62292/njp.v35i2.2026.551

How to Cite

Sunu, S. A., Oniku, A. S., & Idi, B. Y. (2026). Geospatial and Aeromagnetic investigation of structural lineaments in the Adamawa/Taraba region, upper Benue trough, NE Nigeria: An Implication for Geo-hazard occurrence. Nigerian Journal of Physics, 35(2), 150-167. https://doi.org/10.62292/njp.v35i2.2026.551

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