Geochemical Properties of Kalambaina Formation: Implication on Limestone and Marlstone Qualities for Industrial Uses, Sokoto Basin, Nigeria

Authors

  • Ola-Buraimo Abdulrazaq Olatunji Federal University Birnin Kebbi, Kebbi State, Nigeria
  • Umar Hamida Federal University Birnin Kebbi, Kebbi State, Nigeria

Keywords:

Lithofacies, Kalambaina Formation, Fossiliferous limestone, Marlstone, Suitable for cement production

Abstract

Authors: Ola-Buraimo Abdulrazaq Olatunji* and Umar Hamida

Received : 12 August 2024/Accepted : 20 September 2024

Six samples were collected from Bua Cement Quarry site of Kalambaina Formation with a view towards determining the geochemical properties of the lithofacies, the industrial qualities and applications of the limestone and marlstone. Field outcrop litho-log description was carried out by noting the composition, textural attributes, fossil content, structures and diagenetic effect. The samples were subjected to geochemical analysis using atomic absorption spectrometry (AAS). Field result shows that Kalambaina sequence varies at the base from sparsely fossiliferous whitish limestone, overlain by light grey fissile shale, subsequently overlain by poorly fossiliferous limestone. The shale is intercalated within the upper and lower limestone beds. The non-fossiliferous limestone is unconformably overlain by sandstone, marlstone and micaceous shale which is unconformably capped by conglomeratic ironstone. The geochemical results that for the clastic facies (sandstone and shale) have SiO2, CaO, and Al2O3 average concentration values of 66.7, 24.43 and 0.03 % respectively. Carbonate sediments have average concentration values in SiO2, CaO and Al2O3 with 1.26, 52.36 and 0.56 % respectively, which implies that the carbonate were marine sourced while the clastic sediments were continentally derived. The CaO and SiO2 values for the limestone (52.36, 1.27 %), and marlstone (50.10, 1.26 %) are at variance due to influx of clastic material into the marine carbonate. A comparison of the Kalambaina carbonate rocks with other deposits in Nigeria shows higher CaO content and lower SiO2 value except Shagamu Limestone (CaO: 59.20 % and SiO2: 5.70 %) with higher concentration values. The kalambaina Limestone has a moderately high CaO value of 54.61 % and low SiO2 content of 1.26 % which make it suitable for cement production, and other industrial purposes.

Downloads

Download data is not yet available.

Author Biographies

Ola-Buraimo Abdulrazaq Olatunji, Federal University Birnin Kebbi, Kebbi State, Nigeria

Department of Geology

Umar Hamida, Federal University Birnin Kebbi, Kebbi State, Nigeria

Department of Geology

References

Ahmad, B.B., Jie, Y. & Pan, J. (2018). Geochemical analysis on major and trace elements of limestone deposit at Kalambaina Formation, Sokoto Basin, North western Nigeria. International Journal of Scientific and Engineering Research, 9, 9, pp. 439-452.

Alagbe, S. A. (2006). Preliminary evaluation of ydrochemistry of the Kalambaina Formation, Sokoto Basin, Nigeria. Environmental Geology, 51(1): 39-45.

Brand, U. (1983). Mineralogy and geochemistry of deep sea clay in the Atlantic Ocean and adjacent Seas and Ocean. Geol. Soc. Amer. Bull. 76: 803-832.

Chave, K. E. (1954). Aspects of the biogeochemistry of magnesium in calcareous marine organisms. Jour. Geol. 62: 266-283.

Dessauvagie, T. F. J. (1975). African geology, Ibadan, Nigeria. Pp. 251-266.

Downie, D. G., Walden, T. & John, F. (1982). Modern Lime-Burning plant at Shapefell. Quarry Management and Product, pp. 163-171.

Ehinola, O. A. Oluwajana, A. & Nwabueze, C.O. (2012). Depositional Environment,

Geophysical Mapping and Reserve Estimation of Limestone Deposit in Arimogija - Okeluse Area, Southestern Nigeria. Research Journal in Engineering and Applied Sciences 1, 1, pp. 7-11

Ekwueme, B .N. (1985). The chemical and industrial quality of limestones and marls on the Calabar Flank, South Eastern Nigeria. Nigerian Journal of Mining and Geology. 22, 1-2, pp. 51-56.

Emmanuel, E.O., Justus, O.I. and Chuka, J.O. (2021). Near-surface characterization of sediments of Sokoto Group exposed around Wamakko Area, Northwester Nigeria: An integrated approach. Geology, Ecology, and Landscape, 5, 2, pp. 81-93.

Hamidu, I., Umar, Z. F., Ibrahim, H. A., Halidu, H. & Haruna, G. M. (2024). High‑resolution sequence stratigraphy of the Maastrichtian‑Paleocene succession in the Sokoto Basin. Arabian Journal of Geosciences, 17, 54, pp. 1-13.

Harrison, O. J., Hudson J. M. & Cannel, B. (1990). Appraisal of High Purity Limestone in England and Wales. A study′ of Resources, N′eeds, Uses and Demands. Part 1 Resources Rep. Brit. Geol. Surv. Wf (92), 19p.

Ikhane, P. R., Folorunso, A. F., Nton, M .E. & Oluwalaanu, J. A. (2009). Evaluations of Turonian limestone formation exposed at NIGERCEM-Quarry, Nkalagu, Southeastern Nigeria: A Geochemical Approach. The Pacific Journal of Science and Technology, 10, 2, pp. 763-771.

Kogbe, C. A. (1973). Geology of the Upper Cretaceous and Lower Tertiary sediments of the Nigerian sector of the Iullemmeden Basin, Geol. Rdsch. 62, pp. 197-211.

Kogbe, C. A. (1976). Outline of the Geology of the Iullemmeden Basin in North-Western Nigeria. In: Geology of Nigeria, (Ed. C. A Kogbe). Elizabethan Published Company Lagos Nigeria, pp. 331-343.

Kogbe C A (1979) Geology of the south-eastern (Sokoto) sector of the Lullemmeden. Basin. Dept. of Geology Ahmadu Bello University, Zaria Bulletin, 32: pp.1–142

Odey, J.U., Ugwu, A.C. and Ekwueme, B.N. (2021). Petrogrography, Geochemistry and Industrial Quality of the Etono Limestone in UGEP southwest, southeastern Nigeria. Global Journal of Geological Sciences 1, pp. 145-153.

Offodile, M.E. (2002). Groundwater study and development in Nigeria, 2nd Edition. Jos: Mecon Geology and Engineering Limited.

Ola-Buraimo, A. O. & Meshack, B. H. (2024). Foraminifera and sequence stratigraphy study of the Early Maastrichtian to Paleocene sediments of Kalambaina Formation, Sokoto Basin, northwestern Nigeria (in press).

Ola-Buraimo, A. O. & Mohammed A. T. (2024). Palynological zonation and age dating of the Gamba (Middle Eocene) and Kalambaina (Early Maastrichtian-Paleocene) Formations, Sokoto Basin, northwestern Nigeria (in press).

Olaide, M.A. (1988). Raw Materials for Cement Production after the Year 2000: Availabity, Suitability and Accessibility. National Workshop on Cement and Allied Products. Abeokuta, Nigeria.

Petters, S.W. (1978). Stratigraphic evolution of the Benue Trough and its implication for the Upper Cretaceous palaeogeography of West Africa. Journal of Geology, 86, pp. 311-322.

Petter, S. W. (1980). Biostratigraphy of ufzper Cretaceous Foraminifera of the Benue Trough, Nigeria. Journal of Foraminiferal Research, 10, pp. 91-204.

Petters, S. W. (1982). Central West African Cretaceous-Tertiary Benthic Foraminifera and stratigraphy. Palaeontographica Abteilung, 179, pp. 1-104.

Reyment, R. A. (1965). Aspects of the Geology of Nigeria. Ibadan University Press, 133p.

Downloads

Published

2024-09-30