Neogenní a kvartérní sedimenty v oblasti Nového Hrádku (západní část NP Podyjí)

0522237 - ÚGN 2020 RIV CZ cze J - Článek v odborném periodiku
Nehyba, S. - Kirchner, Karel - Kuda, František
Neogenní a kvartérní sedimenty v oblasti Nového Hrádku (západní část NP Podyjí).
[Neogene and Quaternary deposits in the closest surroundings of the Nový Hrádek (the Podyjí National Park).]
Geologické výzkumy na Moravě a ve Slezsku. Roč. 26, 1-2 (2019), s. 49-57. ISSN 1212-6209
Institucionální podpora: RVO:68145535
Klíčová slova: Lower Miocene * Quaternary * provenance analysis * depositional environment
Obor OECD: Geology
Způsob publikování: Open access
https://journals.muni.cz/gvms/article/view/11832

Neogene deposits of the Carpathian Foredeep were newly recognized in the sedimentary succession within the outcrop close to Nový Hradek site in the area of the Podyjí National Park covered by extensive Quaternary deposits. Facies analysis shows that the recognised Neogene beds represent fluvial deposits. Two facies associations were identified within the Quaternary deposits. Although both of them are interpreted as colluvial deposits, they were formed by a series of gravity flows with highly varied water content. Comparison of Neogene and Quaternary deposits in the surroundings of Nový Hrádek and occurrences of similar sediments within the National Park Thayatal in Austria (e.g. surroundings of Merkersdorf) might provide a further data about the poorly known history of the area during Neogene.

Neogene deposits of the Carpathian Foredeep were newly recognized in the sedimentary succession within the outcrop close to Nový Hradek site in the area of the Podyjí National Park covered by extensive Quaternary deposits. Facies analysis shows that the recognised Neogene beds represent fluvial deposits. Two facies associations were identified within the Quaternary deposits. Although both of them are interpreted as colluvial deposits, they were formed by a series of gravity flows with highly varied water content. Comparison of Neogene and Quaternary deposits in the surroundings of Nový Hrádek and occurrences of similar sediments within the National Park Thayatal in Austria (e.g. surroundings of Merkersdorf) might provide a further data about the poorly known history of the area during Neogene.
Trvalý link: http://hdl.handle.net/11104/0306763