|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, more
Pennsylvanian, Lower; Marine
|Authors|| || Top |
- Vandenberghe, N.E.
- Bouckaert, J.
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.