par Mercier, Éric E.;De Putter, Thierry ;Herbosch, Alain ;Mansy, Jean-Louis
Référence Geologische Rundschau, 83, 1, page (170-179)
Publication Publié, 1994-03
Référence Geologische Rundschau, 83, 1, page (170-179)
Publication Publié, 1994-03
Article révisé par les pairs
Résumé : | The kinematics of internal structuration in the ≪Gaux thrust sheet≫ (Charleroi Coal basin; Belgium) is explained with the help of a geometric model. This model is controlled by the distribution of ≪ Landelies red breccia ≫ outcrops that was syntectonically deposited, probably during the Namurian. We suggest that the tectono-sedimentary evolution was controlled by (1) the growth of a Fault-propagation fold, (2) the formation of collapse structures and (3) localized interbed extension. © 1994 Springer-Verlag. |