| NEHYBA, Slavomír, Katarina HOLCOVÁ, Przemysław GEDL a Nela DOLÁKOVÁ. The Lower Badenian transgressive-regressive cycles – a case study from Oslavany (Carpathian Foredeep, Czech Republic). Neues Jahrbuch für Geologie und Paläontologie. Stuttgart, roč. 279, č. 2, s. 209-238. ISSN 0077-7749. doi:10.1127/njgpa/2016/0548. 2016. |
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@article{1332884,
author = {Nehyba, Slavomír and Holcová, Katarina and Gedl, Przemysław and Doláková, Nela},
article_location = {Stuttgart},
article_number = {2},
doi = {http://dx.doi.org/10.1127/njgpa/2016/0548},
keywords = {facies analyses-provenance-foraminifera-calcareous nannoplankton-dinoflagellate cysts-shoreline position},
language = {eng},
issn = {0077-7749},
journal = {Neues Jahrbuch für Geologie und Paläontologie},
title = {The Lower Badenian transgressive-regressive cycles – a case study from Oslavany (Carpathian Foredeep, Czech Republic)},
volume = {279},
year = {2016}
}
TY - JOUR
ID - 1332884
AU - Nehyba, Slavomír - Holcová, Katarina - Gedl, Przemysław - Doláková, Nela
PY - 2016
TI - The Lower Badenian transgressive-regressive cycles – a case study from Oslavany (Carpathian Foredeep, Czech Republic)
JF - Neues Jahrbuch für Geologie und Paläontologie
VL - 279
IS - 2
SP - 209-238
EP - 209-238
SN - 00777749
KW - facies analyses-provenance-foraminifera-calcareous nannoplankton-dinoflagellate cysts-shoreline position
N2 - 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.
ER -
NEHYBA, Slavomír, Katarina HOLCOVÁ, Przemysław GEDL a Nela DOLÁKOVÁ. The Lower Badenian transgressive-regressive cycles – a case study from Oslavany (Carpathian Foredeep, Czech Republic). \textit{Neues Jahrbuch für Geologie und Paläontologie}. Stuttgart, roč.~279, č.~2, s.~209-238. ISSN~0077-7749. doi:10.1127/njgpa/2016/0548. 2016.
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