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Numerous brittle deformations related to the Late Cretaceous inversion of the Mid-Polish Trough (MPT) have been identified in its various parts using seismic data. The role of Zechstein evaporitic deposits during basin evolution and inversion is also described. A model for the Pomeranian segment of the MPT has been constructed that includes significant decoupling between pre-Zechstein basement and Mesozoic sedimentary infill. In areas without significant influence of Zechstein deposits on tectonic processes, classical inversion structures have been interpreted like reverse faults and uplifted basement blocks. Thickness reductions and local angular unconformities pointing to syn-tectonic sedimentation often accompany these inversion structures. Correlation of well and seismic data allows for fairly precise dating of the inversion activity in various parts of the MPT. For the NW segment indirect observations suggest that inversion activity spanned Turonian to Campanian times, whereas in SE segment inversion could have started in Coniacian, was active in Santonian and Campanian, and reached its peak in Maastrichtian times. Inversion along the NE boundary of the MPT (Koszalin-Chojnice tectonic zone) was associated with strike-slip movements. In this area the first stage of the inversion-related uplift of axial part of the MPT can be dated as post-Turonian and pre-Maastrichtian, the second stage, related to strike-slip movements, as middle Maastrichtian. Maastrichtian is also the age of transverse strike-slip activity along Gŕojec fault. All these dates generally conform to the main compressive events within the Alpine-Carpathian orogenic belt, which suggests some sort of mechanical coupling between this orogenic belt and its foreland.

Mid-Polish Trough inversion &#8211; seismic examples, main mechanisms, and its relationship to the Alpine-Carpathian collision

Mid-Polish Trough inversion – seismic examples, main mechanisms, and its relationship to the Alpine-Carpathian collision