1.
Stratigraphy of the Lower Palaeozoic of the Brabant Massif, Belgium. Part I: The Cambro-Ordovician from the Halle and Ottignies groups
The presumed Upper Ordovician green rocks at Rebecq re-interpreted as a resurfacing of the Cambrian Oisquercq Formation (Senne Valley, Anglo-Brabant deformation belt, Belgium)
The supposed thrust fault in the Dyle-Thyle outcrop area (southern Brabant Massif, Belgium) re-interpreted as a folded low-angle extensional detachment
Sedimentology of the belgian frasnian carbonate platform ; Sédimentologie de la plate-forme carbonatée frasnienne belge
