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MAFFE GRANDHAN - Service géologique de Wallonie

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Synclinorium <strong>de</strong> Dinant (Belgique) au Famennien supérieur :un modèle <strong>de</strong> bassin sédimentaire reconstitué par une analysepluridisciplinaire sédimentologique et micropaléontologique.Me<strong>de</strong>d. Rijks Geol. Dienst, vol. 28, pp. 17-32.Th o r e z, J. & Dr e e s e n, R., 1986. A mo<strong>de</strong>l of a regressive <strong>de</strong>positionalsystem around the Old Red continent as exemplified bya field trip in the Upper Famennian « Psammites du Condroz«in Belgium. Ann. Soc. géol. Belg., 109, pp. 285-323.Th o r e z, J., Go e m a e r e, E. & Dr e e s e n, R., 1986. Ti<strong>de</strong> - andwave-influenced <strong>de</strong>positional environments in the Psammitesdu Condroz (Upper Famennian) in Belgium. In : <strong>de</strong> Boer & coll.(Eds) : ti<strong>de</strong>-influenced sedimentary environments and facies.Rei<strong>de</strong>l Publ. Co., pp. 389-415.Tsi e n, H.H., 1974. Paleoecology of middle Devonian andFrasnien in Belgium. Intern. Symp. Belg. Micropal. Limits,Namur, pub. 12, 53p, Bruxelles.Va n d e r s l e y e n, P., Co e n, M., Ge va e rt s, H. & Le c l e r c q, J.,1967. Atlas <strong>de</strong>s grottes <strong>de</strong> Belgique. Inst. Roy. Sc. Nat. Belg.Va n o v e r s c h e l d e, A., 1994. Les mines <strong>de</strong> pyrite et <strong>de</strong> plomb<strong>de</strong> Heure-en-Famenne. Syndicat d’initiative et <strong>de</strong> tourisme <strong>de</strong>Somme-Leuze.57

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