Les orthogneiss calco-alcalins de Foumban–Bankim : témoins d'une zone interne de marge active panafricaine en cisaillement

The mylonitic rocks of the Central Cameroonian Shear Zone (Foumban–Bankim sector) are mainly ancient magmatic rocks emplaced in an internal zone of a Pan-African active margin. They display calc-alkaline affinities with granitoids of northern Cameroon, but differ by their higher K contents and shoshonitic nature. This spatial distinction in pre- to syn-orogenic magmatism permits to define a north to south potassium increase trend, compatible with the existence of a northern Pan-African subduction zone. The shearing evolution of this margin is marked by the superposition of two mylonitic foliations and the occurrence of unusual δ-type porphyroclasts. This suggests the interference of two shearing phases operating in opposing sense at a constant direction, under deep and shallow metamorphic conditions, respectively. To cite this article: E. Njonfang et al., C. R. Geoscience 338 (2006).