N. Oszczypko, The Western Carpathian Foredeep - Development of the foreland basin in front of the accretionary wedge and its burial history (Poland), GEOL CARPAT, 49(6), 1998, pp. 415-431
The Early to Middle Miocene Carpathian Foredeep in Poland (PCF) developed a
s a peripheral foreland basin related to the moving Carpathian front. The s
ubsidence of the basin was controlled both by the sediment and thrust-induc
ed load. The main episodes of intensive subsidence in the PCF correspond to
the period of progressive emplacement of the Western Carpathians onto the
foreland plate, with exception of the "dormant" Carpathian frontal thrust d
uring the "Middle Badenian" salinary event when a low subsidence or uplift
took place. The important driving force of tectonic subsidence was the empl
acement of the nappe load related to the subduction roll-back. During that
time the loading effect of the thickening of the Carpathian accretionary we
dge on the foreland plate increased and was followed by progressive acceler
ation of total subsidence. The mean rate of the Carpathian overthrusting, a
nd north to north-east migration of the axis of depocentres reached 12 mm/a
at that time. During the Late Badenian-Sarmatian time the rate of advance
of the Carpathian accretionary wedge was lower than that of pinch-out migra
tion and, as a result, the basin widened. The Miocene convergence of the Ca
rpathian wedge resulted in the migration of depocenters and onlap of the su
ccessively younger deposits onto the foreland plate.