Lithofacies and petrofacies gave clues on depositional and tectonic settings.
The sandstones are essentially feldspathic and arkosic arenites.
Provenance area is the uplifted continental block related to a rifted Benue Trough.
Amasiri Sandstone is a product of storm (mass flow) and tidal shelf processes.
Paleoclimatic evaluation indicates semi-arid to semi-humid climatic regimes.