The Lower Badenian transgressive-regressive cycles - a case study from Oslavany (Carpathian Foredeep, Czech Republic)
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11310%2F16%3A10333181" target="_blank" >RIV/00216208:11310/16:10333181 - isvavai.cz</a>
Nalezeny alternativní kódy
RIV/00216224:14310/16:00089307
Výsledek na webu
<a href="http://dx.doi.org/10.1127/njgpa/2016/0548" target="_blank" >http://dx.doi.org/10.1127/njgpa/2016/0548</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1127/njgpa/2016/0548" target="_blank" >10.1127/njgpa/2016/0548</a>
Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
The Lower Badenian transgressive-regressive cycles - a case study from Oslavany (Carpathian Foredeep, Czech Republic)
Popis výsledku v původním jazyce
Two newly drilled boreholes (OSL-1 and OSL-2) at Oslavany (Carpathian Foredeep, Czech Republic, a holostratotype of the Moravian/Lower Badenian) provide data documenting the processes of the Lower Badenian marine transgression and regression along the passive margin of the peripheral foreland basin (south-eastern margin of the Bohemian Massif). Three facies associations show the evolution of the deposition and distinct basin margin paleogeography. Deposits of marine transgression (transgressive lag) are followed by open-marine (outer to inner shelf) deposits interpreted as transgressive and highstand systems tract. They reflect a cratonward shift of the coastline. The topmost foreshore and upper shoreface deposits (falling stage systems tract) recorded forced regression and basinward shift of the shoreline. The recorded transgressive-regressive cycle was induced by the coincidence of global TB 2.4. sea-level cycle and forebulge subsidence. The identified higher-frequency cycles were interpreted as climatically controlled.
Název v anglickém jazyce
The Lower Badenian transgressive-regressive cycles - a case study from Oslavany (Carpathian Foredeep, Czech Republic)
Popis výsledku anglicky
Two newly drilled boreholes (OSL-1 and OSL-2) at Oslavany (Carpathian Foredeep, Czech Republic, a holostratotype of the Moravian/Lower Badenian) provide data documenting the processes of the Lower Badenian marine transgression and regression along the passive margin of the peripheral foreland basin (south-eastern margin of the Bohemian Massif). Three facies associations show the evolution of the deposition and distinct basin margin paleogeography. Deposits of marine transgression (transgressive lag) are followed by open-marine (outer to inner shelf) deposits interpreted as transgressive and highstand systems tract. They reflect a cratonward shift of the coastline. The topmost foreshore and upper shoreface deposits (falling stage systems tract) recorded forced regression and basinward shift of the shoreline. The recorded transgressive-regressive cycle was induced by the coincidence of global TB 2.4. sea-level cycle and forebulge subsidence. The identified higher-frequency cycles were interpreted as climatically controlled.
Klasifikace
Druh
J<sub>x</sub> - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)
CEP obor
DB - Geologie a mineralogie
OECD FORD obor
—
Návaznosti výsledku
Projekt
—
Návaznosti
I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace
Ostatní
Rok uplatnění
2016
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název periodika
Neues Jahrbuch für Geologie und Palaontologie - Abhandlungen
ISSN
0077-7749
e-ISSN
—
Svazek periodika
279
Číslo periodika v rámci svazku
2
Stát vydavatele periodika
DE - Spolková republika Německo
Počet stran výsledku
30
Strana od-do
209-238
Kód UT WoS článku
000370602600006
EID výsledku v databázi Scopus
2-s2.0-84996956158