Szczegóły publikacji
Opis bibliograficzny
The youngest deposits infilling the Gdów "embayment" (Carpathian orogenic front, south Poland) are not older than late Sarmatian-Pannonian / Antoni Wójcik, Małgorzata Garecka, Tomasz Malata, Monika PILARZ // Geological Quarterly ; ISSN 1641-7291. — 2021 — vol. 65 no. 2 art. no. 22, s. 1-15. — Bibliogr. s. 13-15. — Publikacja dostępna online od: 2021-05-21
Autorzy (4)
- Wójcik Antoni
- Garecka Małgorzata
- Malata Tomasz
- AGHPilarz Monika
Słowa kluczowe
Dane bibliometryczne
| ID BaDAP | 135549 |
|---|---|
| Data dodania do BaDAP | 2021-09-06 |
| Tekst źródłowy | URL |
| DOI | 10.7306/gq.1593 |
| Rok publikacji | 2021 |
| Typ publikacji | artykuł w czasopiśmie |
| Otwarty dostęp |  |
| Creative Commons | |
| Czasopismo/seria | Geological Quarterly |
Abstract
The Gdow "embayment" is the most pronounced deflection along the northern boundary of the Carpathians. It is filled by the sandy clay deposits which used to be named the Skawina Formation or Chodenice beds or, locally, conglomerates (of Sypka Gora). Their stratigraphic position according to studies of foraminifers had been determined as Badenian. New results obtained from micropalaeontological material sampled at three exposures near Wiatowice, Jawczyce (Giewont) and Gdow (Sypka Gora), and based on boreholes, indicate a much younger age of for the deposits infilling the Gdow "embayment". These studies show that the surface deposits are not older than Late Sarmatian/Pannonian (Serravalian/Tortonian). They also suggest a much later time for the last stages of the thrusting of the Carpathian Mountains over the Carpathian Foredeep.