Szczegóły publikacji
Opis bibliograficzny
Paleoenvironmental changes in Upper Cretaceous formations in the Polish segment of the Carpathian Foreland / A. Łaba-Biel, A. KWIETNIAK, A. Urbaniec, K. Filipowska-Jeziorek // W: 84th EAGE annual conference & exhibition [Dokument elektroniczny] : June 5–8, 2023, Vienna, Austria. — Wersja do Windows. — Dane tekstowe. — [Vienna] : European Association of Geoscientists & Engineers, 2023. — S. [1-5]. — Wymagania systemowe: Adobe Reader. — Tryb dostępu: https://www.earthdoc.org/content/papers/10.3997/2214-4609.202... [2025-03-26]. — Bibliogr., Summ. — Dostęp do pełnego tekstu po zalogowaniu
Autorzy (4)
- Łaba-Biel Anna
- AGHKwietniak Anna
- Urbaniec Andrzej
- Filipowska-Jeziorek Kinga
Dane bibliometryczne
| ID BaDAP | 158943 |
|---|---|
| Data dodania do BaDAP | 2025-04-23 |
| DOI | 10.3997/2214-4609.202310961 |
| Rok publikacji | 2023 |
| Typ publikacji | materiały konferencyjne (aut.) |
| Otwarty dostęp |  |
Abstract
In the scope of our project, we made an approach to link 3D seismic image and geological information from wells to reconstruct, as detailed as possible, the paleoenvironment of the studied segment of the Upper Cretaceous basin in the central part of the Carpathian Foredeep (Poland), based on the chronostratigraphic method. For depositional systems recognition, seismic attributes were incorporated. The interpretation was performed simultaneously with Wheeler diagrams analysis and interpretation of geological data from the wells. The analysis shows various paleomorphological elements within the studied segment of the Upper Cretaceous basin that affect the type and diversity of sedimentation. The significant influence of tectonic processes on the depositional history of the sedimentary basin was also evidenced. The proposed approach based on chronostratigraphic image and Wheeler diagram analysis in combination with tectonostratigraphic interpretation allowed for detailed recognition of the sedimentary paleoenvironment and reconstruction of the depositional and tectonic history of the analysed segment of the Carpathian Foreland basin. The depositional and tectonic history of the Upper Cretaceous series analysed is related both to regional processes, occurring throughout the Late Cretaceous sedimentary basin, and to local manifestations of small-scale tectonics.
