Study utilizes aeromagnetic data to assess basement depths in a geologically complex region, suggesting critical insights into subsurface structures.
The Yola Arm of the Upper Benue Trough in Nigeria is a geologically complex region with limited subsurface data, hindering a detailed understanding of its basement configuration and sedimentary architecture. This study employs high-resolution aeromagnetic data to estimate basement depths and characterize subsurface structural variations using both spectral analysis and Source Parameter Imaging (SPI). The aeromagnetic data were processed with standard corrections, Reduction to the Equator (RTE), and regional-residual separation to enhance anomaly interpretation. Spectral analysis of 28 overlapping blocks identified shallow magnetic sources ranging from 0.10 to 0.95 km (average 0.55 km), typically associated with intrusive bodies or mineralized zones, and deeper sources from 0.70 to 3.20 km (average 1.95 km), likely corresponding to structural depressions and variable sediment thickness. SPI results revealed depths from 160 m to over 3,400 m, highlighting significant basement heterogeneity. Depth variations are consistent with fault-controlled horst-and-graben structures, reflecting rift-related tectonics and differential sediment accumulation. Integration of the spectral and SPI methods provides a reliable characterization of basement morphology, indicating basement uplifts in the northwestern and central areas and deeper sub-basins in the southeastern parts.
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Kenda et al. (2026) studied this question.
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