SYNTECTONIC HALOKINESIS IN THE VISEAN STR ATA OF THE VARISCAN ALLOCHTONE ARDENNAIS (YVES-GOMEZEE QUARRY, PHILIPPEVILLE AREA, BELGIUM)

Citation
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
Citations number
22
Categorie Soggetti
Multidisciplinary Sciences
ISSN journal
07644450
Volume
318
Issue
1
Year of publication
1994
Part
2
Pages
117 - 121
Database
ISI
SICI code
0764-4450(1994)318:1<117:SHITVS>2.0.ZU;2-J
Abstract
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.