Determination of Basement Depth Using Aeromagnetic SourceParameter Imaging Constraints on The StructuralFramework and its Implications for Geo-Hazard Occurrence in The Upper Benue Trough, NE Nigeria
DOI:
https://doi.org/10.14419/24s4as93Published
27-05-2026Keywords:
SPI; Geo-Hazards; Basement Depth; Upper Benue Trough; LineamentsAbstract
This study investigates the basement depth and structural framework of the Upper Benue Trough, northeastern Nigeria, using high-resolution aeromagnetic data integrated with Source Parameter Imaging (SPI) techniques to assess their implications for geo-hazard occurrence. The aeromagnetic data were processed using Oasis Montaj software 8.9 through standard procedures, including reduction to the equator and regional-residual separation, to enhance subsurface structural features. The SPI method, based on the analytic signal of magnetic sources, was employed to estimate depths to magnetic sources, revealing significant spatial variability ranging from approximately 98 m shallow depths to over 2200 m deeper depths. The results indicate a structurally complex terrain characterized by NE-SW and NW-SE trending fault systems, with deeper sedimentary depocenters concentrated in the central and southern parts of the study area and shallower basement highs along the margins. Integration of SPI-derived depths with lineament density analysis highlights zones of intense fracturing, deformation and structural weakness, which correspond to areas prone to geo-hazards such as flooding, subsidence, landslides, and erosion. The findings reveal that basement configuration and fault-controlled structures play a critical role in controlling geo-hazard susceptibility, providing a critical geophysical framework for improved risk assessment, land-use planning, and sustainable infrastructure development in the Upper Benue Trough.
References
Arthaud MH, Caby R, Fuck RA, Dantas EL, Parente CV (2008). Geology of the northern Borborema Province, NE Brazil, and its correlation with Nigeria, NW Africa. Geol Soc Lond Spec Publ 294(1):49–67. https://doi.org/10.1144/ sp294.4.
Blakely, R. J. (1995). Potential Theory in Gravity and Magnetic Applications. Cambridge University Press. https://doi.org/10.1017/CBO9780511549816.
Blakely, R. J. (1988). Curie temperature isotherm analysis and tectonic implications of aeromagnetic data from Nevada. Journal of Geophysical Re-search, 93(B10), 11817–11832. https://doi.org/10.1029/JB093iB10p11817.
Benkhelil J, Mascle J, Guiraud M (1998). Sedimentary and structural characteristics of the Cretaceous along the Co ˆte D’Ivoire–Ghana transform margin and the Benue trough: A comparison. In: Mascle J, Lohmann GP, Moullade M et al (eds) Proceedings of the ocean drilling program, scientifi c results, vol 159. Ocean Drilling Program, College Station, pp 93–99. https://doi.org/10.2973/odp.proc.sr.159.007.1998.
Benkhelil, J. (1989). The origin and evolution of the Cretaceous Benue Trough, Nigeria. Journal of African Earth Sciences, 8(2–4), 251–282. https://doi.org/10.1016/S0899-5362(89)80028-4.
Connard, G., Couch, R., & Gemperle, M. (1983). Analysis of aeromagnetic measurements from the Cascade Range in central Oregon. Geophysics, 48(3), 376–390. https://doi.org/10.1190/1.1441476.
Eze, O. E., Okiwelu, A. A., Ekwok, S. E., et al. (2024). Delineation of deep-seated crustal structures from magnetic data in the southeastern part of the Niger Delta basin, Nigeria. Frontiers in Earth Science, 12, 1439199. https://doi.org/10.3389/feart.2024.1439199.
Fairhead, J. D., & Binks, R. M. (1991). Differential opening of the Central and South Atlantic Oceans and the opening of the West African rift sys-tem. Tectonophysics, 187(1–3), 191–203. https://doi.org/10.1016/0040-1951(91)90419-S.
Guiraud, R., & Bosworth, W. (1997). Senonian basin inversion and rejuvenation of rifting in Africa and Arabia: Synthesis and implications to plate-scale tectonics. Tectonophysics, 282(1–4), 39–82. https://doi.org/10.1016/S0040-1951(97)00212-6
García-Abdeslem, J., & Ness, G. E. (1994). Variations of Curie depth in southern Mexico using spectral analysis of aeromagnetic data. Geophysics, 59(3), 449–456.
Hinze, W. J., Von Frese, R. R. B., & Saad, A. H. (2013). Gravity and magnetic exploration: Principles, practices, and applications. Cambridge Uni-versity Press. https://doi.org/10.1017/CBO9780511843129.
Li, Y., & Oldenburg, D. W. (1998). 3-D inversion of magnetic data. Geophysics, 63(1), 109–119. https://doi.org/10.1190/1.1444302.
Kearey, P., Brooks, M., & Hill, I. (2002). An introduction to geophysical exploration (3rd ed.). Blackwell Science.
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. Explora-tion Geophysics, 24(4), 679–688. https://doi.org/10.1071/EG993679.
Nabighian, M. N., Grauch, V. J. S., Hansen, R. O., LaFehr, T. R., Li, Y., Peirce, J. W., Phillips, J. D., & Ruder, M. E. (2005). The historical devel-opment of the magnetic method in exploration. Geophysics, 70(6), 33ND–61ND. https://doi.org/10.1190/1.2133784
Ndikum, E. N., & Tabod, C. T. (2024). Applying Source Parameter Imaging (SPI) to aeromagnetic data to estimate depth to magnetic sources in the Mamfe Sedimentary Basin. International Journal of Geosciences, 15, 1–11. https://doi.org/10.4236/ijg.2024.151001
Nabighian, M. N. (1972). The Analytic Signal of Two-Dimensional Magnetic Bodies with Polygonal Cross-section. Geophysics, 37(3), 507–517. https://doi.org/10.1190/1.1440276.
Ofoegbu, C. O. (1985). Curie point depths in Nigeria and their implications for geothermal exploration. Geophysical Journal International, 80(2), 391–408.
Okubo, Y., Graf, R. J., Hansen, R. O., Ogawa, K., & Tsu, H. (1985). Curie point depths of the island of Kyushu and surrounding areas, Japan. Geo-physics, 50(3), 481–494. https://doi.org/10.1190/1.1441926.
Okubo, Y., & Matsunaga, T. (1994). Curie point depth in northeast Japan and its correlation with regional thermal structure and seismicity. Journal of Geophysical Research, 99(B11), 22363–22371. https://doi.org/10.1029/94JB01336.
Pedersen, L. B. (1991). Relations between potential field anomalies and their gradient transformations. Geophysics, 56(6), 884–897. https://doi.org/10.1190/1.1443129.
Reid, A. B., Allsop, J. M., Granser, H., Millett, A. J., & Somerton, I. W. (1990). Magnetic interpretation in three dimensions using Euler deconvolu-tion. Geophysics, 55(1), 80–91. https://doi.org/10.1190/1.1442774.
Salem, A., Williams, S., Fairhead, J. D., Smith, R., & Ravat, D. (2014). Interpretation of magnetic data using tilt-angle derivatives. Geophysics, 79(1), J1–J12. https://doi.org/10.1190/1.2799992.
Shuey, R. T., Schellinger, D. K., Tripp, A. C., & Alley, L. B. (1977). Curie depth determination from aeromagnetic spectra. Geophysical Journal In-ternational, 50(1), 75–101. https://doi.org/10.1111/j.1365-246X.1977.tb01325.x.
Silva, C. A., Bezerra, F. H. R., & Oliveira, L. F. S. (2006). Depth estimation using source parameter imaging of magnetic data. Journal of Applied Geophysics, 60(2), 133–144.
Spector, A., & Grant, F. S. (1970). Statistical models for interpreting aeromagnetic data. Geophysics, 35(2), 293–302. https://doi.org/10.1190/1.1440092.
Sebastian A S., Adetola S O., & Bello Y I. (2026). Geospatial and Aeromagnetic Investigation of Structural Lineaments in the Adamawa/Tarrasa re-gion, Upper Benue Trough, NE Nigeria: An Implication for Geohazard Occurrence. Nigerian Journal OF Physics NJP Volume 35(2) .nipngr.org; https://doi.org/10.62292/njp.v35i2.2026.551.
Tanaka, A., Okubo, Y., & Matsubayashi, O. (1999). Curie point depth based on spectrum analysis of magnetic anomaly data in East and Southeast Asia. Tectonophysics, 306(3–4), 461–470. https://doi.org/10.1016/S0040-1951(99)00072-4.
Telford, W. M., Geldart, L. P., & Sheriff, R. E. (1998). Applied geophysics (2nd ed.). Cambridge University Press.
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(3):807–813. doi:10.1190/1.1444190.
Ugwu, G. Z., & Alasi, T. K. (2016). Aeromagnetic survey for determining depth to magnetic source of Abakaliki and Ugep areas of the Lower Be-nue Trough, Nigeria. Engineering and Technology Journal, 1(1), 1–9.
Yenne, E. Y., Green, C. M., & Torvela, T. (2025). Modelling geologic features and structures in the Middle and Lower Benue Trough of Nigeria from gravity and aeromagnetic data sets. Journal of African Earth Sciences, 231, 105745. https://doi.org/10.1016/j.jafrearsci.2025.105745.
