Geo-Investigation for Gold Mineralisation Veins in Part of Kushaka Schist Belts, Niger State Nigeria, using an integrated approach

Authors

  • A.A. ADETONA
  • K.A. SALAKO
  • O.I. OLARIONYE
  • A.A. ALABI
  • A.A. RAFIU
  • U.D. ALHASSAN

DOI:

https://doi.org/10.33003/fjorae.2025.0201.06

Keywords:

Hydrothermal zones,, F-Parameter,, K-deviation,, Minna-Kushaka Schist belt

Abstract

The research attempt to delineate the exact position and depth to gold loads within sheets 164_Minna on latitude 9.30’ to 10.00 North and longitude 6.30’ to 7.00 East at the terminal end of Minna-Kushaka schist belt. The research employed magnetic, radiometric and very low frequency methods. Eight structural lineaments labelled F1 to F8 where mapped from magnetic data, these structures resulted from the deformation of the basement metamorphic rocks when intrude by volcanic intrusions. Majority of these faultiness area trending in the NE-SW direction. The Hydrothermal altered zones was investigated  using K/eTh ratio, K_deviation and F_parameter derived from the Radiometric data, Regions with values Potasium-ratio_Thorium (K/Th) ranging from 0.3 – 0.5 %/ppm, K_deviation from 7.3 to 60.6 and F_Parameter from 0.8 to 1.3 respectively were delineated as having being considerably altered.  A comprehensive analysis of these results, was used to produce a ternary image in which the delineated region of hydrothermal altered zones appearing in whitish and grey colour located around Minna and Tudun-Fulani, Shakwatu, Shekwata, Gunnu, Sarkin- Pawa, Shiroro, Gunni and Fuka villages. Euler analysis determine the of depths deposits ranging from 5 to 88 metres. Coincidentally mining activities are currently in progress around Shakwatu, Shekwata, Asha, Sarkin- Pawa which falls within the regions delineated. In view of the above, the study recommends the exploration for gold mineral along the profiles VLF A, VLF B, VLF C, VLF D, VLF E, VLF F, VLF G, VLF H, VLF I, VLF J and VLF K respectively. The highest hydrothermal signature correlates with biotite gneiss zones intruded by quartz schist, typical hosts for orogenic gold. The research indicated that location of potentials correlate to the region where exploration is currently going on and beyond, findings from this study can support safer and more efficient resource extraction with minimal environmental impact.

 

References

Abd El Nabi, S. H. (2013). Role of γ-ray spectrometry in detecting potassic alteration associated with Um Ba’anib granitic gneiss and metasediments, G. Meatiq area, Central Eastern Desert, Egypt. Arabian Journal of Geosciences, 6, 1249-1261. https://doi.org/10.1007/s12517-011-0378-4

Adams, J. S., & Gasparini, P. (1970). Methods in Geochemistry and Geophysics.-Gamma-Ray Spectrometry of Rocks. Elsevier.

Adeleke, A. A., Nemakhavhani, T. W., & Popoola, A. P. I. (2014). Evaluation of the Cyanidation Leaching of Gold in a Waste Rock Ore. Iran. J. Chem. Chem. Eng. Vol, 33(2).

Adetona, A. A., Fidelis, I. K., & Shakarit, B. A. (2023). Interpreting the magnetic signatures and radiometric indicators within Kogi State, Nigeria for economic resources. Geosystems and Geoenvironment, 2(2), 100157. https://doi.org/10.1016/j.geogeo.2022.100157

Agterberg, F. P., & Bonham-Carter, G. F. (1999, October). Logistic regression and weights of evidence modeling in mineral exploration. In Proceedings of the 28th international symposium on applications of computer in the mineral industry (APCOM), Golden, Colorado (Vol. 483, p. 490).

Airo, M. L. (2002). Aeromagnetic and aeroradiometric response to hydrothermal alteration. Surveys in Geophysics, 23, 273-302.

Ajibade, A. C., & Wright, J. B. (1989). The Togo-Benin-Nigeria Shield: evidence of crustal aggregation in the Pan-African belt. Tectonophysics, 165(1-4), 125-129.

Akinlalu, A. A. (2023). Radiometric mapping for the identification of hydrothermally altered zones related to Gold mineralization in Ife–Ilesa schist belt, southwestern Nigeria. Indonesian Journal of Earth Sciences, 3(1), A519-A519.

Allen, R. L. (1995). Atlas of Alteration. A Field and Petrographic Guide to Hydrothermal Alteration Minerals. Geological Association of Canada, Mineral Division.

Aliyu, S.B., Adetona, A. A., Adewuyi, R. A., Jude, E., Adewumi, T. (2021). Delineating and interpreting the gold veins within Bida and Zungeru Area, Niger State Nigeria, using aeromagnetic and radiometric data. Pakistan Journal of Geology. DOI: https://doi.org/10.2478/pjg-2021-0006

An, P., Moon, W. M., & Rencz, A. (1991). Application of fuzzy set theory for integration of geological, geophysical and remote sensing data. Canadian Journal of Exploration Geophysics, 27(1), 1-11.

Augie, A. I., & Ologe, O. (2020). Analysis of Aeromagnetic Data for Coal Deposit Potential over Birnin Kebbi and its Environs Northwestern Nigeria. Nigerian Journal of Science and Environment, 18(1), 145.

Bierlein, F. P., Fuller, T., Stüwe, K., Arne, D. C., & Keays, R. R. (1998). Wallrock alteration associated with turbidite-hosted gold deposits. Examples from the Palaeozoic Lachlan Fold Belt in central Victoria, Australia. Ore Geology Reviews, 13(1-5), 345-380.

Cunha, L. O., Dutra, A. C., & Costa, A. B. (2017). Use of radiogenic heat for demarcation of hydrothermal alteration zones in the Pernambuco-Brazil. Journal of Applied Geophysics, 145, 111-123.

Danbatta, U. A. (2008). Precambrian crystal development in the northerwestern part of Zuru schist belt, northwestern Nigeria. Journal of Mining and Geology, 44(1), 45-56.

Danbatta, U. A. (2005). Precambrian crustal development of the northwestern part of Zuru schist belt, NW Nigeria. In A paper presented at the 41st Annual Conference of Nigerian Mining, and Geos. Soc.(NMGS).

Danjumma, S. G., Senchi, D. B., Sale, L., Mohammed, A., & Tudu, A. M. B. (2019). Identification of Mineral Deposits in Garin Awwal Mining Site, Kebbi State, North-Western Nigeria. environment, 6(6).

de Quadros, T. F., Koppe, J. C., Strieder, A. J., & Costa, J. F. C. (2003). Gamma-ray data processing and integration for lode-Au deposits exploration. Natural Resources Research, 12, 57-65.

Dickson, B. L., & Scott, K. M. (1997). Interpretation of aerial gamma-ray surveys-adding the geochemical factors. AGSO Journal of Australian Geology and Geophysics, 17.

Efimov, A. V. (1978). Multiplikativnyj pokazatel dlja vydelenija endogennych rud poaerogamma-spektrometriceskim dannym. Metody rudnoj geofiziki. Leningrad, Naucno-proizvodstvennoje objedinenie geofizika.

Eleraki, M., Ghieth, B., Abd-El Rahman, N., & Zamzam, S. (2017). Hydrothermal zones detection using airborne magnetic and gamma ray spectrometric data of mafic/ultramafic rocks at Gabal El-Rubshi area, Central Eastern Desert (CED), Egypt. Advances in Natural and Applied Sciences, 11(9), 182-197.

Fanton, G., Martinez, M. P., & Gimenez, M. E. (2011, August). AeroGammaspectrometry for Lode-Au Deposits Exploration In Western Pampean Ranges-Argentine. In 12th International Congress of the Brazilian Geophysical Society & EXPOGEF, Rio de Janeiro, Brazil, 15–18 August 2011 (pp. 1124-1129). Society of Exploration Geophysicists and Brazilian Geophysical Society.

Garba, I. (2000). Gold prospect of the Nigerian Pan-African terrain of West Africa. J. Min. Geol, 36(2), 123-126.

Garba, I. (2002). Late Pan-African tectonics and origin of gold mineralization and rare-metal pegmatities in the Kushaka schist belt, northwestern Nigeria. Journal of mining and geology, 38(1), 1-12. https: //doi.org/10.4314/jmg. v38i1 .18768

Garba, I. (2003). Geochemical characteristics of mesothermal gold mineralisation in the Pan-African (600±150 Ma) basement of Nigeria. Applied Earth Science, 112(3), 319-325.

Galbraith, J. H., & Saunders, D. F. (1983). Rock classification by characteristics of aerial gamma-ray measurements. Journal of Geochemical Exploration, 18(1), 49-73.

Geosoft (2009) Grav/Mag interpretation. Montaj extension developed by Geosoft (Electronic version); Oasis Montaj Data Processing Analysis (DPA) system for Earth sciences applications. Euro Technologies.

Jambon, J. L. (2007). Wall Rock Alteration, Geological Survey of Canada, Ottawa

Kwaghhua, F. I., Adetona, A. A., Aliyu, S. B. (2021). Interpretation of major structures within the basement region of Benue-Niger confluence from Aeromagnetic and Radiometric data Kogi state Nigeria. Geological Behavior (GBR) 2021. DOI: 10.26480/gbr.01.2021.17.22

Li, X. (2008). Magnetic reduction-to-the-pole at low latitudes: Observations and considerations. The leading edge, 27(8), 990-1002.

Maden, N., & Akaryalı, E. (2015). Gamma ray spectrometry for recognition of hydrothermal alteration zones related to a low sulfidation epithermal gold mineralization (eastern Pontides, NE Türkiye). Journal of Applied Geophysics, 122, 74-85.

Ministry Of Mines and Steel Development (2010). Gold Deposits Exploration in Nigeria. (n.d). Retrieved from http://www.mmsd.gov.ng/gold/ 2010.

Olugbenga, T. T., & Augie, A. I. (2020). Estimation of crustal thickness within the Sokoto Basin, North-Western Nigeria using bouguer gravity anomaly data. International Journal of Geological and Environmental Engineering, 14(9), 247-252.

Pires, A. C. B. (1995). Identificação geofísica de áreas de alteração hidrotermal, Crixás-Guarinos, Goiás. Brazilian Journal of Geology, 25(1), 61-68.

Quadros, T. D. (2000). Integraçoã de dados para pesquisa mineral de ouro em ambiente SIG na Ilha Cristalina de Rivera, Uruguai (Doctoral dissertation, Tese de Doutoramento, PPGEM, Escola de Engenharia: Universidade Federal do Rio Grande do Sul, PortoAlegre, 260p).

Reid, A. B., Allsop, J. M., Granser, H., Millett, A. T., & Somerton, I. W. (1990). Magnetic interpretation in three dimensions using Euler deconvolution. Geophysics, 55(1), 80-91.

Sanusi, S. O., & Amigun, J. O. (2020a). Structural and hydrothermal alteration mapping related to orogenic gold mineralization in part of Kushaka schist belt, North-central Nigeria, using airborne magnetic and gamma-ray spectrometry data. SN Applied Sciences, 2, 1-26.

Sanusi, S. O., & Amigun, J. O. (2020b). Logistic-based translation of orogenic gold forming processes into mappable exploration criteria for fuzzy logic mineral exploration targeting in the Kushaka schist belt, North-central Nigeria. Natural Resources Research, 29(6), 3505-3526.

Sani, D. G., Senchi, D. B., Sale, L., Mohammed, A., & Tudu, A. M. B. (2019). Identification of Mineral Deposits in Garin Awwal Mining Site, Kebbi State, North-Western Nigeria. environment, 6(6).

Saunders, D. F., Terry, S. A., & Thompson, C. K. (1987). Test of national uranium resource evaluation gamma-ray spectral data in petroleum reconnaissance. Geophysics, 52(11), 1547-1556.

Thompson, D. T. (1982). EULDPH: A new technique for making computer-assisted depth estimates from magnetic data. Geophysics, 47(1), 31-37.

Yannah, M., Suh, C. E., & Mboudou, M. G. M. (2015). Quartz veins characteristics and Au mineralization within the Batouri Au District, East Cameroon. Sci. Res, 3(4), 137149. https://doi.org/10.11648/j.sr.20150304

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Published

2025-07-05