par Préat, Alain 
;Mamet, Bernard
Référence Bulletin des Centres de recherches exploration-production Elf-Aquitaine. Mémoire, 13, 1, page (47-86)
Publication Publié, 1989
;Mamet, Bernard Référence Bulletin des Centres de recherches exploration-production Elf-Aquitaine. Mémoire, 13, 1, page (47-86)
Publication Publié, 1989
Article révisé par les pairs
| Résumé : | A sedimentological model for the Givetian carbonate succession of the Dinant and Namur basins enables recognition of 13 major microfacies. They range from the open marine, below wave action zone, to reefal complexes, lagoons, and evaporitic sabkhas. The rhythmic sedimentation is primarily controlled by subsidence which is in turn counterbalanced by algal carbonate production. -from English summary |
