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Research article
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21 Mar 2022
Research article |
| 21 Mar 2022
| 21 Mar 2022
Deep vs. shallow – two contrasting theories? A tectonically activated Late Cretaceous deltaic system in the axial part of the Mid-Polish Trough: a case study from southeast Poland
Zbyszek Remin
CORRESPONDING AUTHOR
Faculty of Geology, University of Warsaw, Al. Żwirki i Wigury 93, 02-089 Warsaw, Poland
Michał Cyglicki
Faculty of Geology, University of Warsaw, Al. Żwirki i Wigury 93, 02-089 Warsaw, Poland
Polish Geological Institute – National
Research Institute, Rakowiecka 4, 00-975 Warsaw, Poland
Mariusz Niechwedowicz
Faculty of Geology, University of Warsaw, Al. Żwirki i Wigury 93, 02-089 Warsaw, Poland
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Short summary
Traditionally, the axial part of the Polish Basin, i.e. the Mid-Polish Trough, was interpreted as the deepest and most subsiding part of the basin during the Cretaceous times. We interpret this area conversely, as representing a landmass – the Łysogóry–Dobrogea Land. Inversion-related tectonics, uplift on the one hand and enhanced subsidence on the other, drove the development of the Szozdy Delta within the axial part of the basin. New heavy mineral data suggest different burial histories.
Traditionally, the axial part of the Polish Basin, i.e. the Mid-Polish Trough, was interpreted...
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