[ meld een fout in dit record ]

mandje (0): toevoegen | toon

---

Données palynologiques nouvelles dans l'Ordovicien inférieur du bassin de la Senne, Massif du Brabant, Belgique Vanguestaine, M. (1978). Données palynologiques nouvelles dans l'Ordovicien inférieur du bassin de la Senne, Massif du Brabant, Belgique. Ann. Soc. géol. Belg. (1968) 100: 193-198 In: Annales de la Société géologique de Belgique. Vaillant-Carmanne: Liège. ISSN 0037-9395, meer

---

Beschikbaar in	Auteur
VLIZ: Open access 276972 [ download pdf ]

---

Trefwoorden

Geological time > Phanerozoic > Paleozoic > Palaeozoic > Ordovician Acritarcha [WoRMS] Brabant wallon (Province) [Marine Regions]; Genappe [Marine Regions]; Ottignies-Louvain-la-Neuve [Marine Regions]; Rebecq [Marine Regions]; Tubize [Marine Regions]; Villers-la-Ville [Marine Regions] Marien/Kust

---

Auteur		Top
Vanguestaine, M., meer

---

Abstract

The massive phyllites of Oisquercq in the Senne Basin are followed up by quartz phyllites which have yielded acritarchs of several different ages for the different localities, viz. Arenig or Llanvirn at Asquempont (Brussels-Charleroi canal section), lower Tremadoc at Virginal (railway cutting north of Virginal Station), Arenig or Lanvirn at Quenast (railway cutting east of Quenast). These new micropalaeontological data show the existence of two quartz phyllitic intervals in the Senne Basin, and suggest the correlation of the first with the " quartzophyllades" of Chévlipont, and the second with the "quartzophyllades" of the Abbey of Villers-la-Ville of the Dyle Basin. They thus provide support for Fourmarier's opinion that the grey, variegated and green rocks of Oisquercq would be the stratigraphie equivalent, in different facies, of the black rocks-of Mousty.

---

Alle informatie in het Integrated Marine Information System (IMIS) valt onder het VLIZ Privacy beleid

Top | Auteur