Abstract

This report describes the experiences obtained in the well drilled recently near Stekene. This well has been drilled within the scope of a study of the Belgian Geological Survey (BGS) on the extension of Oligocene and Eocene formations. During drilling of the well cores have been taken across the entire sandy unit, which consists of both the Berg Sand Member and the sandy top of the Kallo Complex. Samples of these cores were analysed on their permeability, porosity and density.