Neogene and Quaternary deposits in the closest surroundings of the Nový Hrádek (the Podyjí National Park)

Result code in IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F68145535%3A_____%2F19%3A00522237" target="_blank" >RIV/68145535:_____/19:00522237 - isvavai.cz</a>

Alternative codes found

RIV/00216224:14310/19:00111678

Result on the web

<a href="https://journals.muni.cz/gvms/article/view/11832" target="_blank" >https://journals.muni.cz/gvms/article/view/11832</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.5817/GVMS2019-1-2-49" target="_blank" >10.5817/GVMS2019-1-2-49</a>

Result language

čeština

Original language name

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

Original language description

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.

Czech name

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

Czech description

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.

Type

J_SC - Article in a specialist periodical, which is included in the SCOPUS database

CEP classification

—

OECD FORD branch

10505 - Geology

Project

—

Continuities

I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Publication year

2019

Confidentiality

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Name of the periodical

Geologické výzkumy na Moravě a ve Slezsku

ISSN

1212-6209

e-ISSN

—

Volume of the periodical

26

Issue of the periodical within the volume

1-2

Country of publishing house

CZ - CZECH REPUBLIC

Number of pages

9

Pages from-to

49-57

UT code for WoS article

—

EID of the result in the Scopus database

2-s2.0-85079221579