Pre-permian sedimentation in NW Europe - pre-Permian depositional-environments around the brabant massif in Belgium, the Netherlands and Germany
Bless, M.J.M.; Bouckaert, J.; Conil, R.; Groessens, E.; Kasig, W.; Paproth, E.; Poty, E.; Vansteenwinkel, M.; Streel, M.; Walter, R. (1980). Pre-permian sedimentation in NW Europe - pre-Permian depositional-environments around the brabant massif in Belgium, the Netherlands and Germany. Sediment. Geol. 27(1): 1-81. dx.doi.org/10.1016/0037-0738(80)90031-7
In: Sedimentary Geology. Elsevier: Tokyo; Oxford; New York; London; Amsterdam. ISSN 0037-0738; e-ISSN 1879-0968, meer
Pre-Permian sedimentation in northwestern Europe has been controlled by the structural evolution of this area. Cambro-Silurian deposition has been influenced by partly synsedimentary movements (among others Ordovician-Silurian uplift south of the Brabant/Condroz zone, such as the Stavelot-Venn Massif).Presence, respectively absence of important late Caledonian deformation has subdivided northwestern Europe into three major sedimentary environments during the Devono-Carboniferous: the Caledonian fold belt and the Cornwall-Rhenish Basin which are separated by the Belgo-Dutch platform.Subsequently, the Hercynian or Variscan orogenies have gradually reduced the sedimentary area and produced the overall withdrawal of the marine environment. Eventually, large-scale overthrusts - such as the Dinant Nappe - masked parts of the original sedimentary basins.
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