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Summary

The Benue Trough is an elongate rifted depression in which the sediments reach well over 5000 m thickness in places and have been strongly folded, probably by later adjustments along faults in the underlying basement. The Bida Basin is a shallow unfaulted arm of the Benue Trough. The Benue Trough probably provided the major link between the Mediterranean (Tethys Ocean) and Gulf of Guinea via the lullmedden and Chad Basins, during Upper Cretaceous times.

The Niger Delta at the southern end of the Benue Trough has been building out into the Atlantic since the end of the Cretaceous. Of the other coastal basins, the Senegal Basin is by far the largest, but the basins along the southern coast of West Africa are larger than their surface extents suggest, as substantial parts of their successions are offshore.

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© 1985 J. B. Wright, D. A. Hastings, W. B. Jones & H. R. Williams

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Wright, J.B. (1985). The Benue Trough and coastal basins. In: Wright, J.B. (eds) Geology and Mineral Resources of West Africa. Springer, Dordrecht. https://doi.org/10.1007/978-94-015-3932-6_11

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  • DOI: https://doi.org/10.1007/978-94-015-3932-6_11

  • Publisher Name: Springer, Dordrecht

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