Rotated joints in folded Magura flysch (Polish Flysch Carpathians)
Authors
Antoni K. Tokarski
Abstract
Zrotowany cios w sfałdowanym fliszu jednostki magurskiej
In the Outer Carpathian flysch the variability of dihedral angle between transverse complementary joint sets is structurally controlled. In the Krynica tectonic unit the dihedral angle augments gradually outwards attaining maximum values near the overthrust surface. This may be explained toy internal rotation due to flexural-flow folding.
