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Une faune à conodontes du tournaisien dans le massif de la Vesdre
Boonen, P. (1978). Une faune à conodontes du tournaisien dans le massif de la Vesdre. Ann. Soc. géol. Belg. (1968) 101: 127-130
In: Annales de la Société géologique de Belgique. Vaillant-Carmanne: Liège. ISSN 0037-9395, more
Peer reviewed article  
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Keywords
    Geological time > Phanerozoic > Paleozoic > Palaeozoic > Carboniferous
    Geological time > Phanerozoic > Paleozoic > Palaeozoic > Carboniferous > Mississippian, Lower > Tournaisian
    Conodonta
    Belgium, Limburg [Marine Regions]; Belgium, Lontzen [Marine Regions]; Belgium, Pepinster [Marine Regions]
    Marine/Coastal
Author  Top 
  • Boonen, P.
Abstract
    A conodont fauna is recorded from the Etroeungt and Pont d'Arcole Formations and from the base of the Landelies Formation in the Vesdre Massif ofBelgium. It is proposed to retain the name "Dolomie de la Vesdre" for the dolomites situated above the basal part of the Landelies Formation. This unit is the same as the "Obere Dolomit" in the German part of the massif.
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