Simplified lithostratigraphy of the Outer Polish Carpathians (after Koszarski et al., 1985; Dziadzio et al., 2001; modified) with the position of field trip stops

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... nappes became uprooted from the basement and only their basinal parts were preserved. The succession of the nappes from the lowest to the highest is as follows (concordant to our trip -from north to south): Skole (Skiba) Nappe (mainly easternmost part of Carpathians), Subsilesian Nappe, Silesian Nappe, Fore-Magura group of nappes and Magura Nappe (Fig. 8). We discuss here main units ...

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... jer & Wieser, 1990;). Lower Cretaceous Urgonian-type exotic rocks often occur within such gravelstones (Bukowiny Gravelstone Member -Birkenmajer & Lefeld, 1969) which represents a submarine slump, in the middle of the Sromowce Formation of the Niedzica Succession (Birkenmajer, 1977(Birkenmajer, , 1979Birkenmajer & Jed- norowska, 1987b) (Fig. ...

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... to decreasing amount of food, which in turn is related to deepening of sea of the Pieniny Klippen Basin from Early to Late Jurassic, according to the general trend in this part of the Tethys. https://journals.agh.edu.pl/geotour Stop 15 -Baška village -part of the Hradiště Formation with so-called teschenite volcanics (including pillow lavas) (Fig. 48) (Petr Skupien, Zdeněk Vašíček) Late Jurassic subsidence enhanced deposition in several troughs (from south to north the Magura-, the Silesianand the Subsilesian basins) separated by ridges. During Early Cretaceous, black shale dysoxic sedimentation with local submarine clastic fans embraced almost all Outer Carpathian basins. Slow and ...