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ISSN Print: 2381-1099 ISSN Online: 2381-1102

International Journal of Geophysics and Geochemistry

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Geochemical and Geophysical Investigations of Kaolin Deposits of the Maastrichtian Mamu Formation, Northern Anambra Basin, Nigeria

International Journal of Geophysics and Geochemistry
Vol.5 , No. 2, Publication Date: May 30, 2018, Page: 45-52

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Authors

[1]	Baba Yahaya, Department of Earth Sciences, Kogi State University, Anyigba, Nigeria.
[2]	Omali Aurelius Ojoina, Department of Earth Sciences, Kogi State University, Anyigba, Nigeria.
[3]	Usman Ayatu Ojonugwa, Department of Earth Sciences, Kogi State University, Anyigba, Nigeria.

Abstract

Geochemical and Geophysical investigation of clay deposits at Ofe-Jiji, Aloji and Udane-Biomi, Northern Anambra Basin, has been carried out in a view of delineating the chemical contents and the thickness of the clay deposit within the study area. Geochemical analysis of the clay deposits were carried out using Minipal 4 XRF Analyser to analyse the chemical contents of the clay deposits while the vertical electrical sounding of the Schlumbergier arrays was used to delineate the lithologic unit across the mapped area. Results of the geochemical analysis reveals that SiO₂ and Al₂O₃ are the major oxides found in the clay deposits. SiO₂ is 65.91% at Ofe-Jiji, 61.53% at Aloji and 70.59% at Udane-Biomi. Al₂O₃ has a reverse trend to SiO₂ ranging from 19.42% at Ofe-Jiji to 21.72% at Aloji, and 16.67% at Udane-Biomi. Minor oxides are Fe₂O₃, MgO, CaO, Na₂O, K₂O, TiO₂, MnO, V₂O₅ and Cr₂O₃. Geochemical parameters, such as Al₂O₃/TiO₂ and SiO₂/Al₂O₃ ratios suggest that the 3 kaolin deposits studied have been derived from intermediate source rocks. Results from the geophysical interpretation show that the average thicknesses of the clay unit at Ofe-Jiji, Aloji and Undane Boimi are 62.7 meters, 14.1 meters and 9.7 meters respectively and the average resistivity values of the clay unit in each of the location are 554.33 Ωm, 583.15 Ωm and 421.77 Ωm. The geochemical results also show that the kaolins meet the criteria for use as, ceramic and brick clay raw materials.

Keywords

Geochemical Analysis, Resistivity Survey, Clay Minerals, Kaolinite, Provenance, Conductivity

Reference

[01]	Akaegbobi, I. M. (2005). The crab eye view of the organic sedimentological evolution of the Anambra Basin, Nigeria: Hydrocarbon source potential and economic implications. Faculty of Science Lecture University of Ibadan, Ibadan, 42.
[02]	Akhirevbulu, O. E., Amadasun, C. V. O., Ogunbajo, M. I. and Ujuanbi O. (2010). The Geology and Mineralogy of clay occurrences Around Kutigi Central Bida Basin, Nigeria. Ethiopia Journal of Environmental Studies and Management 3 (3), 49-56.
[03]	Badmus, B. S and Olatinsu, O. B. (2009). Geophysical evaluation and chemical analysis of Kaolin clay deposit of Lakiri Village, south Western Nigeria. International Journal of Physical sciences. 4 (10) 592-606.
[04]	Emufurieta, W. O. (1988). A Comparative Study of two Kaolin Deposits in South Western Nigeria. Journ. Min. and Geosc. 24, 15-20.
[05]	Ezeh, C. C., 2008. Hydrogeoelectrical estimation of aquifer parameters in Enugu State Nigeria. Unpubl. PhD dissertation, University of Nigeria, Nsukka.
[06]	Fatai, O. A., Kenneth, K. A., Peter A. O and Joseph O. B (2014). Characterization of some clay deposits in South West Nigeria. Leonardo Electronic Journal of Practices and Technologies. Issue 25, p. 46-57
[07]	Henriet, J. P., 1977. Direct Application of Da- Zarrouk Parameters in Groundwater Surveys. Geophysical Prospecting. vol. 24, pp 344-353.
[08]	Ibrahim, A. G., Okoli, O. G and Dahiru, D (2016). Comparative Study of the Properties of Ordinary Portland Cement Concrete and Binary Concrete Containing Metakaolin Made from Kankara Kaolin in Nigeria. ATBU Journal of Environmental Technology 9 (5) P 53-59
[09]	Keller, G. V. and Frischnechk, F. C., 1979. Electrical Methods in Geophysical Prospecting. Program Press: New York, NY. Pp 91-135.
[10]	Kurkura et al., (2012). Mineralogical and geochemical characterization of clay and lacustrine deposits of Lake Ashenge Basin, northern Ethiopia: Implication for industrial applications. Momona Ethiopia Journ. Of Sc.(MJS), 4 (2); 111-129.
[11]	Mark, U. and Onyema Obi, O. O. (2009). Assessment of the Industrial Potentials of some Nigerian Kaolinitic Clay Deposits. Inter. Res. E. Journal of clay deposits.
[12]	Mongelli, G., Cullers, R. L., Muelheisen, S., (1996). Geochemistry of Late Cretaceous- Oligocenic shales from Varicolori Formation, southern Apennines, Italy: Implication for mineralogical, grain-size control and provenance. Eur. J. Mineral. 8, 733-754.
[13]	Nwajide, C. S. and Reijers, T. J. A. (1996). Geology of the Southern Anambra Basin. In: Reijers, T. J. A. (Ed), Selected chapters on Geology, SPDC, Warri, pp. 133-148.
[14]	Obaje, N. G. (2009). Geology and mineral resources of Nigeria. 1^st edition Springer Books, Heidelberg. 60-62.
[15]	Okunlola, O. A and Olubunmi. I (2012). The geochemistry of claystone-shale deposits from the Maastritchian Patti formation, Southern Bida basin, Nigeria. Earth Sci. Res. S. J. 16 (2), 57-67.
[16]	Reijers, T. J. A and Nwajide, C. S. (1998). Geology of the Southern Anambra Basin. Unpublshed Report for Chevron Nigeria Limited, Field Course Note 66p.
[17]	Short, K. C. and Stauble, A. J. (1968). Outline of Geology of Niger Delta. Bul. Amer. Ass. Petr. Geol. Vol. 54 (5) 761-779.
[18]	Taylor, J. H. (1951). Clay Minerals and the Evolution of Sedimentary Rocks. Paper Read 2^nd November 1951.
[19]	Umeji, P. O. (2005). Palynological study of the Okaba coal section in the Anambra Basin, Southern Nigeria, Journ. of Mining and Geol. 41 (2), pp. 194.
[20]	Weaver, C. E., (1953). Mineralogy and petrology of some Ordovician K-bentonites and related limestones: Geol. Soc. Amer. Bull. V. 64, Pp. 921-943.