Géologie du synclinal de l'Itombwe (Zaïre oriental) et le problème de l'existence d'un sillon plissé pan-africain

Abstract

From the N.S. linear structure of the Itombwe syncline arise some problems in central Africa. Some authors considered it as a Kibarian structure and others as an isolated fold belt of Pan-African orogeny. This ambiguity is the result, in its greatest part, of the scarceness of field work and the lack of dating on the rocks of this syncline. A study on the central area showed the existence of two lithostructural units. The western area is correlated with a Kibarian structure while the eastern area had some similarities with the tectonic Pan-African troughts from NE of Zaïre and west of Uganda. The existence of an area folded during the Pan-African orogeny and in the same environment as the great African lakes area must be considered.