Together but separate: decoupled Variscan (late Carboniferous) and Alpine (Late Cretaceous-Paleogene) inversion tectonics in NW Poland

In Europe, formation of the Palaeozoic Variscan orogenic belt, and the Mesozoic-Cenozoic Alpine- Carpathian orogenic belt led to a widespread inversion events within forelands of both orogenic domains. We used legacy 2-D seismic data together with the newly acquired 3-D seismic data that, for the first time, precisely imaged sub-Zechstein (i.e. sub-evaporitic) upper Palaeozoic successions in NW Poland in order to develop a quantitative, balanced 2-D model of the late Palaeozoic-recent evolution of this area, characterised by a complex pattern of repeated extension and inversion. Four main tectonic phases have been determined: (1) Late Devonian-early Carboniferous extension and subsidence possibly related to extensional reactivation of Caledonian thrusts, (2) late Carboniferous inversion caused by the Variscan orogeny, (3) Permo-Mesozoic subsidence related to the development of the Polish Basin and (4) its Late Cretaceous-Paleogene inversion. Variscan and Alpine structures form a superimposed multilayer inversion system, mechanically decoupled by the Zechstein evaporites.

Automated summary

This study uses seismic data to model the geological evolution of Northwest Poland, revealing multiple extension and inversion events in the crust from the late Paleozoic to the present. The findings are significant for understanding the tectonic evolution of this region.