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A somewhat simple stratigraphy has generally been applied to the Congo Basin, with gross subdivision of the Mesozoic-Cenozoic cover sequences into numerous poorly resolved units. The stratigraphy of cover sequences across the basin is ambiguous and poorly resolved as a result of limited studies and inconsistent nomenclature between different regions, poor age controls and ambiguous biostratigraphy that obfuscate the depositional history of the basin.

DOI 10.1007/978-2-2_9 The Congo Basin represents one of the largest and least studied continental sedimentary basins in the world. In 'Geology and Resource Potential of the Congo Basin', editted by M.J. Mesozoic sedimentary cover sequences of the Congo Basin in the Kasai Region, Democratic Republic of Congo. 'Roberts, E., Jelsma, H., Perritt, S., and Hegna, T. The aged equivalent stratigraphic units and lithologies of the West-Congolian (WCB), Katangan (CAC) and Bambuí (SFB) successions are examined, compared and coupled with the available carbon and oxygen isotope values, and a regional correlation is proposed. New δ 13 C and δ 18 O stable isotope data obtained complete the dataset for the Schisto-Calcaire Subgroup in the frame of a correlation with the same succession in Gabon and the Republic of the Congo.

The C3 (Luanza) Formation is subdivided into four submembers and the transition of the C3 Formation with both the C2 and C4 formations is examined.

This work characterizes and reinterprets the stratigraphical succession from the C2 (Bulu) up to the C4 (Lukunga) formations.

New detailed lithological, sedimentological, major chemical, δ 13 C and δ 18 O stable isotopes data were obtained from exploration drilling samples on carbonate formations of the Neoproterozoic Schisto-Calcaire Subgroup (> 635-575 Ma) in the Lukala area (Bas-Congo, Democratic Republic of the Congo).

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