Grain-Size Distribution and Paleohydrodynamic Analysis of the Maastrichtian Ajali Sandstone, Anambra Basin, Nigeria | ||
| Sustainable Earth Trends | ||
| دوره 6، شماره 1، 2026، صفحه 99-113 اصل مقاله (1.74 M) | ||
| نوع مقاله: Original Research Article | ||
| شناسه دیجیتال (DOI): 10.48308/set.2025.238196.1104 | ||
| نویسندگان | ||
| Christian Chukwudi Agbo* ؛ Samuel Okechukwu Onyekuru؛ Diugo Okereke Ikoro؛ Timothy Chibuike Anyanwu | ||
| Geology Department, School of Physical Sciences, Federal University of Technology, Owerri, Nigeria | ||
| چکیده | ||
| The Maastrichtian Ajali Sandstone of the Anambra Basin, southeastern Nigeria, was investigated to assess its grain-size distribution and paleohydrodynamic characteristics, to interpret its depositional environment and flow regime. Twenty representative samples were analyzed for statistical grain-size parameters, including mean grain size (1.29–2.10ϕ), standard deviation (0.41–1.13ϕ), skewness (−0.39 to 0.40ϕ), and kurtosis (0.64–1.50ϕ). These values indicate that the sandstones are coarse to medium-grained, moderately to moderately well sorted, and exhibit both positive and negative skewness, ranging from platykurtic to leptokurtic, indicating deposition under fluctuating high-energy conditions, including channel and possible beach environments. Bivariate and multivariate plots confirm a unidirectional, high-energy fluvial system, while the log-probability curves show mixed transport mechanisms (traction, saltation, and suspension). Paleohydraulic reconstructions suggest flow velocities of 0.5–1.2 m/s, consistent with braided river systems. Provenance analysis further indicates sediment derivation from the nearby Oban Massif and Basement Complex. Collectively, the data indicate that the Ajali Sandstone was deposited in a braided fluvial system influenced by episodic high-energy events in a semi-arid climatic setting, with minor tidal modifications in marginal zones. | ||
| کلیدواژهها | ||
| Fluvial sedimentation؛ Paleoenvironment؛ Sediment transport | ||
| مراجع | ||
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