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Munsterman, D.K. (author), Deckers, J. (author)
Based on palynologic interpretations, the Oligocene/Miocene boundary was identified in the cored samples of the ON-Mol-1 and Weelde boreholes in the southern North Sea Basin. In both boreholes, the presumed location of the Oligocene/Miocene boundary is marked by a thin gravel bed, which testifies of a hiatus, within a continuation of shelly,...
article 2020
Vandenberghe, N. (author), Harris, W.B. (author), Wampler, J.M. (author), Houthuys, R. (author), Louwye, S. (author), Adriaens, R. (author), Vos, K. (author), Lanckacker, T. (author), Matthijs, J. (author), Deckers, J. (author), Verhaegen, J. (author), Laga, P. (author), Westerhoff, W.E. (author), Munsterman, D.K. (author)
The glauconite-rich Diest Formation in central and north Belgium contains sands in the Campine subsurface and the hilly Hageland area that can be distinguished from each other. The Hageland Diest Sands member contains no stratigraphically relevant fossils while in the Campine subsurface dinoflagellate cysts are common and show a stratigraphic...
article 2014