After the mass extinction of colonial reefs in the Ardennes at the Frasnian-Famennian boundary, (crypt)algal-sponge-crinoidal mud mounds suddenly appeared during the mid-Famennian time (Early-Late marginifera Zone) in the Verviers Synclinorium (Eastern Belgium). These carbonate buildups represent the first reported occurrence of mud mounds in the latest Upper Devonian of Western Europe. The mounding sites for the mud mounds (locally known as "the Marbre rouge à crinoïdes de Baelen") are developed on a block-faulted basement.Après l'extinction massive des récifs coralliens des calcaires dévoniens des Ardennes, à la limite Frasnien-Famennien, des monticules de boue (crypt)algaire à éponges, crinoïdes et brachiopodes sont soudainement apparus ...
The facies architecture, sedimentary dynamics and palaeogeographical evolution were reconstructed fo...
peer reviewedThis paper provides a synthetic sedimentological overview of the middle Frasnian carbon...
During the Eifelian and early Givetian, isolated mud mounds were established in a shallow basin, pre...
The Red Marble of Baelen from the Limbourg area (Vesdre Basin, Eastern Belgium) represents a member ...
The "red crinoïdal marble" of Baelen represents a local member of the Souverain-Pré Formation (Middl...
The facies architecture, sedimentary dynamics and palaeogeographic evolution were reconstructed for...
A succession of Frasnian mounds on the southern border of the Dinant Synclinorium (Belgium) was inve...
This paper focuses on the early and middle Frasnian stratigraphic interval from the Ardennes area in...
The Psammites du Condroz (Upper Famennian, Upper Devonian) in Belgium display a complex interfingeri...
The Devonian Coumiac carbonate series is well known since it is the point reference in time for the ...
form in Belgium. Geol. Quart., 48 (3): 253–266. Warszawa. This paper provides a synthetic sedimentol...
This paper provides a synthetic sedimentological overview of themiddle Frasnian carbonate platform o...
Late Frasnian Petit-Mont Member carbonate mounds occur in the southern pail of the Dinant Synclinori...
Stromatoporoids are the most abundant large skeletal organisms in middle Frasnian carbonate mound en...
The facies architecture, sedimentary dynamics and paleogeographic evolution were reconstructed for a...
The facies architecture, sedimentary dynamics and palaeogeographical evolution were reconstructed fo...
peer reviewedThis paper provides a synthetic sedimentological overview of the middle Frasnian carbon...
During the Eifelian and early Givetian, isolated mud mounds were established in a shallow basin, pre...
The Red Marble of Baelen from the Limbourg area (Vesdre Basin, Eastern Belgium) represents a member ...
The "red crinoïdal marble" of Baelen represents a local member of the Souverain-Pré Formation (Middl...
The facies architecture, sedimentary dynamics and palaeogeographic evolution were reconstructed for...
A succession of Frasnian mounds on the southern border of the Dinant Synclinorium (Belgium) was inve...
This paper focuses on the early and middle Frasnian stratigraphic interval from the Ardennes area in...
The Psammites du Condroz (Upper Famennian, Upper Devonian) in Belgium display a complex interfingeri...
The Devonian Coumiac carbonate series is well known since it is the point reference in time for the ...
form in Belgium. Geol. Quart., 48 (3): 253–266. Warszawa. This paper provides a synthetic sedimentol...
This paper provides a synthetic sedimentological overview of themiddle Frasnian carbonate platform o...
Late Frasnian Petit-Mont Member carbonate mounds occur in the southern pail of the Dinant Synclinori...
Stromatoporoids are the most abundant large skeletal organisms in middle Frasnian carbonate mound en...
The facies architecture, sedimentary dynamics and paleogeographic evolution were reconstructed for a...
The facies architecture, sedimentary dynamics and palaeogeographical evolution were reconstructed fo...
peer reviewedThis paper provides a synthetic sedimentological overview of the middle Frasnian carbon...
During the Eifelian and early Givetian, isolated mud mounds were established in a shallow basin, pre...