Le Givetien et le Frasnien du massif de la Vesdre : biostratigraphie et paléogéographie

Thèse de doctorat en sciences -- UCL, 197

Sedimentologie, diagenese et stratigraphie des biohermes de marbre rouge de la partie superieure du Frasnien belge. Compte-rendu de la session extraordinaire des societes geologiques belges les 14 et 15 septembre 1990

A global view of the geology of "F2j' mud mounds from the upper part of the Belgian Frasnian is briefly presented. The paper deals successively with the stratigraphy and the sedimentology of the mounds and the paleogeographic evolution of the Frasnian ramp in relation with eustatism. Diagenetic evolution of buildups and enclosing rocks is also considered. A selection of sections from mound, peri-mound and off-mound environments is described in detail. -English summarySCOPUS: ar.jinfo:eu-repo/semantics/publishe

Highlighting of the Marenne fault on the geological map Aye - Marche-en-Famenne

peer reviewedThe revision of the geological map Aye - Marche-en-Famenne (Belgium, Wallonia, Hotton) has emphasized an important deformation structure named the Marenne Fault. This fault is clearly visible at the southeastern face of the Marenne quarry. The dating by rugose corals has allowed to define with precision the Givetian lithologic units that have been put in contact by this normal faul with a later, right-lateral strike-slip component. This fault, that may be traced over a few kilometers to the East, is probably late Hercynian, of the same type and origin as the Lamsoul Fault know to the South of Marche-en-Famenne. It seems to form part of a family of faults which are regularly observed on the south side of the Dinant Synclinorium.Modernisation de la carte géologique de la Walloni

Highlighting the Marenne fault on the new geological map "Aye - Marche-en-Famenne" (Belgium, Wallonia)

Revision of the geological map Aye-Marche (Belgium, Wallonia) has highlighted a major tectonic fault known as "Marenne fault". Its presence would explain the increased thickness of the Givetian limestones up to the valley of Ourthe river.Révision de la carte géologique de Wallonie - Recherche collective d'intérêt généra

Les formations du Dévonien moyen de la Belgique

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Complexes récifaux et tectonique synsédimentaire dans le Givétien inférieur de Belgique

Communication et Abstract, p 126info:eu-repo/semantics/nonPublishe

Sedimentologie et coraux du bioherme de marbre rouge frasnien (F2j) de Tapoumont (massif de Philippeville, Belgique)

Twelve microfacies range from sponge spicule mudstones to crinoidal, coral rudstones. Water agitation and light supply normally control the bioherm growth, but three environments do not follow the rule. Four lateral microfacies are studies. The bioherm geometry is discussed, and a weak sedimentary slope is proposed. -from English summarySCOPUS: ar.jinfo:eu-repo/semantics/publishe

Compte-rendu de l’excursion de la Société belge de Géologie du 6 novembre 1985 consacrée à l’étude du sommet du Couvinien et du Givétien au bord sud du Bassin de Dinant, de Resteigne à Beauraing

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