Rotated joints in folded Magura flysch (Polish Flysch Carpathians)

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.

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