Two supra-salt faults form a crestal collapse graben in the Glückstadt Graben.
Faults cut the entire post-Permian strata from top of salt into Holocene deposits.
Stratigraphic data indicate that these faults moved mainly in the Cenozoic.
Faults continued developing during the Pleistocene until today.
Recent salt tectonics and fault reactivation due to differential ice-sheet loading