Publisher © Czech Geological Survey, ISSN: 2336-5757 (online), 0514-8057 (print)
Tectonic structure of the south part of the Plzeň Basin
Geoscience Research Reports 35, 2002 (GRR for 2001),
pages 71–72
Abstract
A "solid" exposed map of Carboniferous rocks (Bolsovian - Stephanian C) on the south of the Plzeň basin shows the maximum subsidence and maximum thickness of sediments in to centres of structural low of NNE-SSW direction. The structural low is dislocated by faults forming a system of transverse (with respect to the basin axis) graben and horst structures.
