T. Deputter et al., SYNTECTONIC HALOKINESIS IN THE VISEAN STR ATA OF THE VARISCAN ALLOCHTONE ARDENNAIS (YVES-GOMEZEE QUARRY, PHILIPPEVILLE AREA, BELGIUM), Comptes rendus de l'Academie des sciences. Serie 2, Mecanique, physique, chimie, sciences de l'univers, sciences de la terre, 318(1), 1994, pp. 117-121
The structural and stratigraphic study of the Palaeozoic series of the
Yves-Gomezee quarry (in the ''Allochtone ardennais'') proves that hal
okinetic processes occurred locally in the Franco-Belgian Variscan bel
t. These processes involved Upper Visean (V3a) evaporites, whose later
dissolution caused the brecciation of the host limestones. The import
ance of such processes in the Dinantian tectonics is discussed.