South border of Dinant synclinorium.
Mesodevonian (Givetian-Frasnian) carbonate series.
Mineralization in normal longitudinal EW fractures.
Deposition due to fracture reopening and pressure fall (general distension).
Ref.: Bull. Minéral. , 1984, 107, pp. 227-232.
South border of Dinant synclinorium.
Mesodevonian (Givetian-Frasnian) carbonate series.
Mineralization in normal EW fractures.
Deposition due to fracture reopening and pressure fall (general distension).