New 40Ar/39Ar, fission track and sedimentological data on a middle Miocene tuff layer occurring in the Vienna Basin: Implications for the north-western Central Paratethys region
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11410%2F19%3A10398511" target="_blank" >RIV/00216208:11410/19:10398511 - isvavai.cz</a>
Výsledek na webu
<a href="https://verso.is.cuni.cz/pub/verso.fpl?fname=obd_publikace_handle&handle=c9FOv0V3F2" target="_blank" >https://verso.is.cuni.cz/pub/verso.fpl?fname=obd_publikace_handle&handle=c9FOv0V3F2</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.2478/geoca-2019-0022" target="_blank" >10.2478/geoca-2019-0022</a>
Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
New 40Ar/39Ar, fission track and sedimentological data on a middle Miocene tuff layer occurring in the Vienna Basin: Implications for the north-western Central Paratethys region
Popis výsledku v původním jazyce
The Kuchyňa tuff is found on the Eastern margin of the Vienna Basin and was formed by felsic, possibly phreatomagmatic volcanism. The Ar/Ar single grain sanidine method was applied and resulted in an age of 15.23 +- 0.04 Ma, which can be interpreted as the age of the eruption. The obtained numerical age is in accordance with the subtropical climate inferred by the presence of fossil leaves that originated in an evergreen broadleaved forest. Furthermore, the described volcanism was connected with the syn-rift stage of the back-arc Pannonian Basin system. The sedimentological data from the underlying sandy mudstones indicate alluvial environment what confirms terrestrial conditions during deposition. Moreover, the tuff deposition probably occurred shortly before the Badenian transgression of the Central Paratethys Sea.
Název v anglickém jazyce
New 40Ar/39Ar, fission track and sedimentological data on a middle Miocene tuff layer occurring in the Vienna Basin: Implications for the north-western Central Paratethys region
Popis výsledku anglicky
The Kuchyňa tuff is found on the Eastern margin of the Vienna Basin and was formed by felsic, possibly phreatomagmatic volcanism. The Ar/Ar single grain sanidine method was applied and resulted in an age of 15.23 +- 0.04 Ma, which can be interpreted as the age of the eruption. The obtained numerical age is in accordance with the subtropical climate inferred by the presence of fossil leaves that originated in an evergreen broadleaved forest. Furthermore, the described volcanism was connected with the syn-rift stage of the back-arc Pannonian Basin system. The sedimentological data from the underlying sandy mudstones indicate alluvial environment what confirms terrestrial conditions during deposition. Moreover, the tuff deposition probably occurred shortly before the Badenian transgression of the Central Paratethys Sea.
Klasifikace
Druh
J<sub>imp</sub> - Článek v periodiku v databázi Web of Science
CEP obor
—
OECD FORD obor
10505 - Geology
Návaznosti výsledku
Projekt
—
Návaznosti
I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace
Ostatní
Rok uplatnění
2019
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název periodika
Geologica Carpathica
ISSN
1335-0552
e-ISSN
—
Svazek periodika
2019
Číslo periodika v rámci svazku
70 (5)
Stát vydavatele periodika
SK - Slovenská republika
Počet stran výsledku
19
Strana od-do
386-404
Kód UT WoS článku
000495458600002
EID výsledku v databázi Scopus
2-s2.0-85075205556