Sedimentary and petrofacies analyses of the Amasiri Sandstone, southern Benue Trough, Nigeria: Implications for depositional environment and tectonic provenance
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文摘

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.

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