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Lower Llanvirn (Ordovician) Graptolites and Acritarchs from the "Assise de Huy", bande de Sambre-et-Meuse, Belgium
Servais, Th.; Maletz, J. (1992). Lower Llanvirn (Ordovician) Graptolites and Acritarchs from the "Assise de Huy", bande de Sambre-et-Meuse, Belgium. Ann. Soc. géol. Belg. (1968) 115(1): 265-285
In: Annales de la Société Géologique de Belgique (1968). Vaillant-Carmanne: Liège. ISSN 0037-9395, more
Peer reviewed article  

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  • Servais, Th.
  • Maletz, J.

Abstract
    The Huy formation («assise de Huy») is the oldest unit present in outcrops in the Belgian «Bande de Sambre-et-Meuse». Graptolites and acritarchs show that the beds are of early Llanvirn Didymograptus artus Biozone age. The localities of Huy and of Sart-Bernard and the Wépion borehole are reinvestigated and the collection of Maillieux, 1939 is restudied.

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