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On the origin of the folding in the Namurian strata at the Namur citadelle, Belgium
Vandenberghe, N.E.; Bouckaert, J. (1984). On the origin of the folding in the Namurian strata at the Namur citadelle, Belgium. Sediment. Geol. 37(3): 163-183. dx.doi.org/10.1016/0037-0738(84)90006-X
In: Sedimentary Geology. Elsevier: Tokyo; Oxford; New York; London; Amsterdam. ISSN 0037-0738; e-ISSN 1879-0968, more
Peer reviewed article  
Available in  Authors 
Keywords
    Geological time > Phanerozoic > Paleozoic > Palaeozoic > Carboniferous > Pennsylvanian, Lower
    Marine/Coastal
Authors  Top 
  • Vandenberghe, N.E.
  • Bouckaert, J.
Abstract
    A number of the features of folding at the Namur Citadelle, a classical outcrop of Namurian strata, can be interpreted in terms of penecontemporaneous deformation induced by sandstones overlying shales of lighter density. Variscan tectonics has then overprinted already folded rocks.
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