Provenance Study of A Section of The Lokoja Sandstone,Southern Bida Basin, North-Central Nigeria
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https://doi.org/10.14419/wavpga03
Received date: June 26, 2025
Accepted date: August 10, 2025
Published date: September 6, 2025
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Fluvial Deposition; Granulometric Analysis; Petrography; Subarkosic Sandstone; Sediment Provenance -
Abstract
This study investigates the provenance and depositional environment of the Lokoja Sandstone in the Southern Bida Basin, North-Central Nigeria. The purpose is to determine the compositional maturity, textural characteristics, and source terrain of the sandstone using integrated granulometric and petrographic analyses. Four stratigraphic sections were logged along the Lokoja–Abuja expressway, with representative sandstone samples collected and analyzed. Grain size distribution was assessed through dry sieve analysis, and statistical parameters—mean size, sorting, skewness, and kurtosis were calculated. Thin-section petrography was conducted to evaluate mineral composition and sediment maturity.
The results show that the sandstone is predominantly coarse- to medium-grained, poorly sorted, and positively skewed, with kurtosis values ranging from mesokurtic to leptokurtic—characteristics typical of high-energy fluvial environments. Petrographic analysis reveals a dominance of monocrystalline quartz (87%), with moderate feldspar (12%) and trace muscovite (1%), classifying the sandstone as subarkosic. The presence of subangular grains and feldspar suggests limited chemical weathering.
In conclusion, the Lokoja Sandstone was deposited in a braided river system under variable flow conditions and sourced from the rounding Precambrian Basement Complex. These findings contribute to a better understanding of sediment dispersal and tectono-sedimentary evolution of the Southern Bida Basin.
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How to Cite
Yaqub, R., Oyudo, I. M., Jimoh, M. A. ., Ogunnubi, E. O., & Aluko, M. O. . (2025). Provenance Study of A Section of The Lokoja Sandstone,Southern Bida Basin, North-Central Nigeria. International Journal of Advanced Geosciences, 13(2), 18-27. https://doi.org/10.14419/wavpga03
