An understanding of the displacement patterns (kinematics) of orogenic belts is essential in order to analyze complex regional structural relationships and the tectonic processes involved. This article outlines some results from kinematic studies carried out during the past decade on shear and thrust zones associated with Proterozoic orogenic belts in Central Africa. These data indicate that Proterozoic orogeny is characterized by major horizontal displacements and that previous ideas of dominantly vertical tectonics are not supported.