The Lower Badenian transgressive-regressive cycles – a case
study from Oslavany (Carpathian Foredeep, Czech Republic)

J 2016

The Lower Badenian transgressive-regressive cycles – a case study from Oslavany (Carpathian Foredeep, Czech Republic)

NEHYBA, Slavomír, Katarina HOLCOVÁ, Przemysław GEDL a Nela DOLÁKOVÁ

Základní údaje

Originální název

The Lower Badenian transgressive-regressive cycles – a case study from Oslavany (Carpathian Foredeep, Czech Republic)

Autoři

NEHYBA, Slavomír (203 Česká republika, garant, domácí), Katarina HOLCOVÁ (203 Česká republika), Przemysław GEDL (616 Polsko) a Nela DOLÁKOVÁ (203 Česká republika, domácí)

Vydání

Neues Jahrbuch für Geologie und Paläontologie, Stuttgart, 2016, 0077-7749

Další údaje

Jazyk

angličtina

Typ výsledku

Článek v odborném periodiku

Obor

10500 1.5. Earth and related environmental sciences

Stát vydavatele

Německo

Utajení

není předmětem státního či obchodního tajemství

Impakt faktor

Impact factor: 0.777

Kód RIV

RIV/00216224:14310/16:00089307

Organizační jednotka

Přírodovědecká fakulta

DOI

http://dx.doi.org/10.1127/njgpa/2016/0548

UT WoS

000370602600006

Klíčová slova česky

faciální analýza-provenience-foraminifery-vápnitý nannoplankton-dinoflagellata- pozice břežní čáry

Klíčová slova anglicky

facies analyses-provenance-foraminifera-calcareous nannoplankton-dinoflagellate cysts-shoreline position

Štítky

AKR, rivok

Změněno: 13. 3. 2018 12:44, prof. RNDr. Slavomír Nehyba, Dr.

Anotace

V originále

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.

Citovat

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, 2016, roč. 279, č. 2, s. 209-238. ISSN 0077-7749. Dostupné z: https://dx.doi.org/10.1127/njgpa/2016/0548.

@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, 2016, roč.~279, č.~2, s.~209-238. ISSN~0077-7749. Dostupné z: https://dx.doi.org/10.1127/njgpa/2016/0548.

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