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Geochemistry and Structural Control of Brines in the Middle Benue Trough, Nigeria

Magashi Umar Bashir Nathaniel Gother Goki

Subject area: Science,Engineering and Technology  ·  Area of research: Geology

DOI: https://doi.org/10.64388/IREV9I8-1714149

Abstract

Brine occurrence in the Middle Benue Trough, Nigeria, is strongly influenced by the region’s structural and stratigraphic framework. This study integrates geological mapping, geophysical interpretation and hydro-chemical analysis investigations to assess structural control on brine migration. Field observations reveal that NE–SW and NW–SE trending basement-rooted faults, particularly at intersections and terminations, are the principal pathways for the vertical ascent of mineralized fluids. Aeromagnetic and Source Parameter Imaging (SPI) data confirm the presence of deep fault corridors coinciding with brine-rich localities. Hydro-chemical analyses show extremely high salinity, predominantly Na–Cl facies, and elevated potassium, calcium, and trace metal concentrations, suggesting evaporite dissolution and prolonged water–rock interaction. These evidences, supports a model of structurally focused brine migration and stratigraphic confinement within permeable sandstones such as the Keana Formation. The findings have dual implications: (1) exploration targeting should prioritize fault intersections, anticline closures, and structurally confined porous units for economically valuable brines; and (2) environmental management should focus on monitoring and protecting shallow aquifers in structurally active zones. This multidisciplinary approach provides a robust framework for both resource development and groundwater protection in tectonically complex basins.

Keywords

Aeromagnetic interpretation, Brine migration, Hydrochemistry, Middle Benue Trough, Structural Control

References

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[2] Ekwok, S. E., George, A. M., Omori, A. A., Abdelrahman, K., Ugar, S. I., Andráš, P., Morphy, M. I., Akpan, A. E., & Eldosouky, A. M. (2024). Unveiling the mineral resources and structural patterns in the Middle Benue Trough: a comprehensive exploration using airborne magnetic and radiometric data. Geocarto International, 39(1). https://doi.org/10.1080/10106049.2024.2339290

[3] Ekwok, S. E., George, A. M., Omori, A. A., Abdelrahman, K., Ugar, S. I., Andráš, P., Morphy, M. I., Akpan, A. E., & Eldosouky, A. M. (2024). Unveiling the mineral resources and structural patterns in the Middle Benue Trough: a comprehensive exploration using airborne magnetic and radiometric data. Geocarto International, 39(1). https://doi.org/10.1080/10106049.2024.2339290

[4] Ferguson, G., Lindsay, M. B. J., Jasechko, S., Luijendijk, E., McIntosh, J. C., Grasby, S. E., & Hendry, M. J. (2018). The Persistence of Brines in Sedimentary Basins. Geophysical Research Letters, 45(10), 4851–4858. https://doi.org/10.1029/2018gl078409

[5] Flexer, V., Baspineiro, C. F., & Galli, C. I. (2018). Lithium recovery from brines: A vital raw material for green energies with a potential environmental impact in its mining and processing. Science of The Total Environment, 639, 1188–1204. https://doi.org/10.1016/j.scitotenv.2018.05.223

[6] Joshua, A. K., Anthony John, I., Ikechukwu, E. D., & Ebuka, A. O. (2023). Scrutinate proclivity of regional aquifer hydraulic parameters: apriorisms for borehole failures within parts of the middle Benue Trough, Nigeria. Water Practice & Technology, 18(12), 3347–3364. https://doi.org/10.2166/wpt.2023.211

[7] NSDWQ (2015). Nigerian Standard for Drinking Water Quality. Nigerian Industrial Standards, 16-22.

[8] Offodile, M.E. (1976). The geology of the Middle Benue Trough, Nigeria, Ph.D. Thesis, University of Uppsala, 4:22-136.

[9] Offodile, M.E. (2014). Hydrogeology. Groundwater Study and Development in Nigeria, Third Edition. Published by Mecon Engineering Services Ltd, Ratya, Jos, Nigeria.

[10] Olade, M. A. (1975). Evolution of Nigeria’s Benue Trough (Aulacogen): a tectonic model. Geological Magazine, 112(6), 575–583. https://doi.org/10.1017/s001675680003898x

[11] Osinowo, O. O., Akanji, A. O., Sanuade, O. A., & Esho, O. O. (2023). Hydrocarbon potential evaluation of the Middle Benue Basin, East-Central Nigeria, using high-resolution aeromagnetic data. Results in Geophysical Sciences, 100058, 3-4. Retrieved from https://www.sciencedirect.com/journal/results-in-geophysical-sciences.

[12] Tijani, M. N. (2004). Evolution of saline waters and brines in the Benue-Trough, Nigeria. Journal of Applied Geochemistry, 19, 1356–1365.

[13] WHO (2017). Guidelines for Drinking Water Quality: Fourth Edition, Incorporating the First Addendum, Geneva, Switzerland. 469-47.

[14] Zheng, M., Liu, H., & Wang, Y. (2020). The evolution and utilization of Salt Lake brines in China: A review. Ore Geology Reviews, 119, 103397. https://doi.org/10.1016/j.oregeorev.2020.103397

How to cite this paper

Magashi Umar Bashir, Nathaniel Gother Goki "Geochemistry and Structural Control of Brines in the Middle Benue Trough, Nigeria" Iconic Research And Engineering Journals Volume 9 Issue 8 2026 Page 306-313 https://doi.org/10.64388/IREV9I8-1714149
Magashi Umar Bashir, Nathaniel Gother Goki "Geochemistry and Structural Control of Brines in the Middle Benue Trough, Nigeria" Iconic Research And Engineering Journals, vol. 9, no. 8, Feb. 2026, doi: https://doi.org/10.64388/IREV9I8-1714149
Magashi Umar Bashir, Nathaniel Gother Goki (2026). Geochemistry and Structural Control of Brines in the Middle Benue Trough, Nigeria. Iconic Research And Engineering Journals, 9(8). doi: https://doi.org/10.64388/IREV9I8-1714149
Magashi Umar Bashir, Nathaniel Gother Goki "Geochemistry and Structural Control of Brines in the Middle Benue Trough, Nigeria" Iconic Research And Engineering Journals, vol. 9, no. 8, Feb. 2026. Crossref, https://doi.org/10.64388/IREV9I8-1714149
@article{1714149,
      author = {Magashi Umar Bashir, Nathaniel Gother Goki},
      title = {Geochemistry and Structural Control of Brines in the Middle Benue Trough, Nigeria},
      journal = {Iconic Research And Engineering Journals},
      year = {2026},
      volume = {9},
      number = {8},
      pages = {306-313},
      issn = {2456-8880},
      url = {https://www.irejournals.com/formatedpaper/1714149.pdf},
      abstract = {Brine occurrence in the Middle Benue Trough, Nigeria, is strongly influenced by the region’s structural and stratigraphic framework. This study integrates geological mapping, geophysical interpretation and hydro-chemical analysis investigations to assess structural control on brine migration. Field observations reveal that NE–SW and NW–SE trending basement-rooted faults, particularly at intersections and terminations, are the principal pathways for the vertical ascent of mineralized fluids. Aeromagnetic and Source Parameter Imaging (SPI) data confirm the presence of deep fault corridors coinciding with brine-rich localities. Hydro-chemical analyses show extremely high salinity, predominantly Na–Cl facies, and elevated potassium, calcium, and trace metal concentrations, suggesting evaporite dissolution and prolonged water–rock interaction. These evidences, supports a model of structurally focused brine migration and stratigraphic confinement within permeable sandstones such as the Keana Formation. The findings have dual implications: (1) exploration targeting should prioritize fault intersections, anticline closures, and structurally confined porous units for economically valuable brines; and (2) environmental management should focus on monitoring and protecting shallow aquifers in structurally active zones. This multidisciplinary approach provides a robust framework for both resource development and groundwater protection in tectonically complex basins.},
      keywords = {Aeromagnetic interpretation, Brine migration, Hydrochemistry, Middle Benue Trough, Structural Control},
      month = {February},
      doi = {https://doi.org/10.64388/IREV9I8-1714149}
  }