Delvaux, D. 1985. ‘Géologie et tectonique du Parc de Lesse et Lomme au bord sud du Bassin de Dinant (Rochefort, Belgique)’. Bulletin de la Société géologique de Belgique 94: 81-95. Bruxelles.  (PR).

Article in a scientific Journal / Article in a Journal

Whilst preparing a new geological and structural map of the "Lesse et Lomme" Park (Han-sur-Lesse, Rochefort and Jemelle), we took the opportunity of re-examining the local hercynian tectonic of the south side of the Dinant bassin. The principal tectonic elements occuring are : -major longitudinal structures (N-S or NNW-SSE compression) with folds of several tectonic types; normal, reverse and thrust faults. -minor and late transversal structures, some of which have been caused by a late east-west compression. Details have been collected concerning the Lamsoul fault, which continues westward to Eprave, and the Forrières fault, which has been followed as far as Han-sur-Lesse. The tectonic significance of the "Klippe du Bois de Niau" has been surveyed.