Home > Journals > IRESPUB Journal of Natural & Applied Sciences > Volume 2 Issue 2 > Analysis of high resolution aeroradiometric data over Sokoto basin and adjoining areas northwestern, Nigeria

Year Launched: 2021

Journal Menu

Analysis of high resolution aeroradiometric data over Sokoto basin and adjoining areas northwestern, Nigeria

Volume 2, Issue 2, May-Jun 2022    |  Page 84-96  |  PDF (3MB)  |  Pub. Date: Jun 20, 2022

Author(s)

Kamureyina Ezekiel1* & Ahmed Nur2; 1Geology Department, Adamawa State University, Mubi P. O. BOX 25, Mubi Nigeria.; 2Geology Department Modibbo Adama University, Yola Nigeria.

Abstract

The analysis of high resolution aeroradiometric data over Sokoto basin was carried out to determine the radioactive heat production of the area, with a view of finding geothermal energy source to augment the epileptic power supply being experienced in the country. The findings of this research revealed that the total count map has range of values from 362.332cps to 2571.005cps, Potassium percent values range from 0.11 to 2.036, thorium values range from 3.920ppm to 17.470ppm and Uranium values range from 0.484ppm to 6.322ppm. The qualitative interpretation revealed that uranium, potassium and thorium are abundant in the basement rocks. Quantitative analysis of potassium, thorium and uranium to obtain heat production shows low radioactive heat production values with a range of 0.00036μWm-3 to 0.10490 μWm-3 and moderate radioactive values that range from 0.10490 μWm-3 to 0.16309μWm-3. The findings indicate that the area have low to moderate potentials of radioactive heat production and concentration of radioactive minerals.

Keywords

aeroradiometric data; radioactive heat; potassium concentration; thorium concentration; uranium concentration

Cite this paper

Ezekiel, K., Nur, A. (2022), Analysis of high resolution aeroradiomatric data over Sokoto basin and adjoining areas northwestern, Nigeria, IRESPUB Journal of Natural & Applied Sciences. Volume 2, Issue 2, May-Jun 2022, Page 84-96

References

[1] Ramadas, G., Subhash, B.A., Laxmi, U.G. (2015). Structural Analysis of Airborne Radiometric Data for Identification of Kimberlites in Parts of Eastern Dharwar Craton. International Journal of Science and Research, 4(4), 2375-2380.

[2]Glimore, G. (2008). Practical Gamma Ray Spectroscopy, (2nd ed.) UK. Wiley.

[3] Bristow, C., Williamson, B. (1989). Spectral Gamma Ray Logs: Core to Log Calibration, Facies Analysis and Correlation Problems in the Southern North Sea. Soc. Lond. Spec. Publ. 41:81 – 88.

[4]Davies, S., McLean, D. (1996). Spectral Gamma-Ray and Palynological Characterization of Kinderscoutian Marine Bands in the Namurian of the Pennine Basin. Yorks. Geol. Polytech. Soc., 51, 103-114.

[5] Myers, K., Bristow, C. (1989). Detailed Sedimentology and Gamma-Ray Log Characteristics of a Namurian Deltaic Succession II: Gamma-Ray Logging. Soc. Lond. Spec. Publ. 136, 1-7.

[6]Rybach, L., Hokrick, R., Eugester, W. (1988). Vertical Earth Heat Probe Measurement and Prospects in Switzerland. Communication and Proceedings, 1, 167-372.

[7] Sanderson, D, East, B, Scott, E. (1989). Aerial Radiometric Survey of Parts of North Wales in July 1989. Scottish Universities Research and Reactor Centre. Glasgow, UK.

[8] Mero, J.L., (1960). Uses of the Gamma-Ray Spectrometer in Mineral Exploration. Geophysics, 25, 1054-1076.

[9]Kogbe, C.A. (1976). Outline of the Geology of Illummeden Basin, Geology of Nigeria. Elizabethan Publishing Co. Pp. 331 – 338.

[10] Ali, M., Wagani, I., Handa, M. (2019). Geochemistry and Mineralogy of the Upper Cretaceous-Paleocene Marine Series Iullummeden Basin, Niger Republic. Journal of Geosciences and Environment Protection. Vol. 7, Pp. 1 – 19.

[11] Nigeria Geological Survey Agency, NGSA (2006). Topographic Map of Latitude 110.30– 130.30′ and Longitude 40.00′- 60.00′.

[12] Offodile, M.E. (2002). Ground water study and development in Nigeria (2nd ed.). Mecon Geology and Eng., Services Ltd., Jos Nigeria.

[13] Nigerian Geological Survey Agency, NGSA (2006). Geological Map of Latitude 11030′ – 13030’and Longitude 4000′ and 6000′.

[14] Obaje, G. N., Aduku, M., Yusuf, L. (2013). The Sokoto Basin of Northwestern Nigeria: A Preliminary Assessment of the Hydrocarbon Prospectivity. Petroleum Technology Development Journal, 3(2), 66-80.

[15] Oteze, G. E. (1976). The Hydrogeology of Northwestern Nigeria Basin, in Geology of Nigeria “Edited by Kogbe C. A.” Elizabethan Press. Pub.

[16] Abaa, S. I. (1983). The structure and petrography of alkaline rocks of the Mada Younger Granite Complex, Nigeria. Journal of African Earth Sciences. Vol. 3, Pp. 107-113

[17] Burke, K.C., Dewey, J. F. (1972). Orogeny in Africa. In: Dessauvagie, T. F. J., Whiteman, A. J. (eds), Africa Geology. University of Ibadan Press, Ibadan, 583-608 Complex, Nigeria. Journal of African Earth Sciences, 3:107-113

[18]Gandu, A. H., Ojo, S. B., Ajakaiye, D. E. (1986). A gravity study of the Precambrian rocks in the Malumfashi Area of Kaduna State, Nigeria. Tectonophysics, 126, Pp. 181-194