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The Wissower Bach Syncline on the Jasmund Peninsula (NE Germany) has been examined to understand the complicated glacitectonic environment in the southern Baltic Sea region, comprising folds and thrust faults from the Weichselian–Pleniglacial. Soft‐sediment thin sections from a SW‐dipping thrust fault at the south‐western limb of the syncline between Cretaceous chalk (hangingwall) and Pleistocene...
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