Szczegóły publikacji
Opis bibliograficzny
From shallow to deep marine depositional environments of the Cretaceous northwestern Tethys – a record of Alpine system differentiation in the Polish Carpathians / Jacek Grabowski, Krzysztof Bąk, Marta BĄK, Michał KROBICKI, Damian Lodowski, Alfred Uchman, Jan GOLONKA, Zbigniew GÓRNY, Jan Hejnar, Jolanta Iwańczuk, Barbara Olszewska, Nestor Oszczypko, Dorota Salata, Andrzej Wierzbowski, Patrycja Wójcik-Tabol // W: Cretaceous of Poland [Dokument elektroniczny] : and of adjacent areas : field trip guide / ed. by Ireneusz Walaszczyk, Jordan P. Todes. — Wersja do Windows. — Dane tekstowe. — Warsaw : Faculty of Geology. University of Warsaw, 2022. — e-ISBN: 978-83-944813-5-3. — S. 297–362. — Tryb dostępu: https://tiny.pl/wjjf6 [2023-01-10]. — Bibliogr. s. 354–362, Abstr. — Materiały towarzyszące konferencji 11th international Cretaceous symposium : Warsaw, Poland, [22–26 August] 2022
Autorzy (15)
- Grabowski Jacek
- Bąk Krzysztof
- AGHBąk Marta
- AGHKrobicki Michał
- Lodowski Damian
- Uchman Alfred
- AGHGolonka Jan
- AGHGórny Zbigniew
- Hejnar Jan
- Iwańczuk Jolanta
- Olszewska Barbara
- Oszczypko Nestor
- Salata Dorota
- Wierzbowski Andrzej
- Wójcik-Tabol Patrycja
Dane bibliometryczne
| ID BaDAP | 144388 |
|---|---|
| Data dodania do BaDAP | 2023-01-10 |
| Rok publikacji | 2022 |
| Typ publikacji | materiały konferencyjne (aut.) |
| Otwarty dostęp |  |
| Wydawca | Uniwersytet Warszawski |
Abstract
The Western Carpathians represent a fold-and-thrust belt that forms the northernmost European Alpides in the Czech Republic, Slovakia, and Poland. They consist of an older range, known as the Inner or Central Carpathians, and a younger range, the Outer or Flysch Carpathians, separated by the Pieniny Klippen Belt. The Inner Carpathians are formed of thick- and thin-skinned nappes thrusted in the Late Jurassic and Cretaceous, while the exclusively thin-skinned nappes of the Outer Carpathians originated during the Cenozoic. Both Cretaceous and Neogene tectonic phases affected the Pieniny Klippen Belt. Cretaceous deposits are present in each of the three tectonic domains, representing a variety of environments spanning from pelagic carbonates, hemipelagic marlstones, and flysch-type terrigenous sediments to Urgonian-type platform carbonates.
