Articles | Volume 15, issue 8
https://doi.org/10.5194/se-15-1029-2024
https://doi.org/10.5194/se-15-1029-2024
Research article
 | 
15 Aug 2024
Research article |  | 15 Aug 2024

Post-Caledonian tectonic evolution of the Precambrian and Paleozoic platform boundary zone offshore Poland based on the new and vintage multi-channel reflection seismic data

Quang Nguyen, Michal Malinowski, Stanisław Mazur, Sergiy Stovba, Małgorzata Ponikowska, and Christian Hübscher

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Cited articles

Ahlrichs, N., Hübscher, C., Noack, V., Schnabel, M., Damm, V., and Krawczyk, C. M.: Structural Evolution at the Northeast North German Basin Margin: From Initial Triassic Salt Movement to Late Cretaceous-Cenozoic Remobilization, Tectonics, 39, e2019TC005927, https://doi.org/10.1029/2019TC005927, 2020. 
Ahlrichs, N., Noack, V., Hübscher, C., Seidel, E., Warwel, A., and Kley, J.: Impact of Late Cretaceous inversion and Cenozoic extension on salt structure growth in the Baltic sector of the North German Basin, Basin Res., 34, 220–250, https://doi.org/10.1111/bre.12617, 2022. 
Al Hseinat, M. and Hübscher, C.: Late Cretaceous to recent tectonic evolution of the North German Basin and the transition zone to the Baltic Shield/southwest Baltic Sea, Tectonophysics, 708, 28–55, https://doi.org/10.1016/j.tecto.2017.04.021, 2017. 
Antonowicz, L., Iwanowska, E., and Rendak, A.: Tensional tectonics in the Pomeranian section of the TT Zone and the implications for hydrocarbon exploration, Geol. Q., 38, 289–306, 1994. 
Babel Working Group: Deep Seismic Reflection/Refraction Interpretation of Crustal Structure along Babel Profiles A and B in the Southern Baltic Sea, Geophys. J. Int., 112, 325–343, https://doi.org/10.1111/j.1365-246X.1993.tb01173.x, 1993. 
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Short summary
Our work demonstrates the following: (1) an efficient seismic data-processing strategy focused on suppressing shallow-water multiple reflections. (2) An improvement in the quality of legacy marine seismic data. (3) A seismic interpretation of sedimentary successions overlying the basement in the transition zone from the Precambrian to Paleozoic platforms. (4) The tectonic evolution of the Koszalin Fault and its relation to the Caledonian Deformation Front offshore Poland.