NEHYBA, Slavomír, Katarina HOLCOVÁ, Przemysław GEDL and 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, vol. 279, No 2, p. 209-238. ISSN 0077-7749. Available from: https://dx.doi.org/10.1127/njgpa/2016/0548.
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Basic information
Original name The Lower Badenian transgressive-regressive cycles – a case study from Oslavany (Carpathian Foredeep, Czech Republic)
Authors NEHYBA, Slavomír (203 Czech Republic, guarantor, belonging to the institution), Katarina HOLCOVÁ (203 Czech Republic), Przemysław GEDL (616 Poland) and Nela DOLÁKOVÁ (203 Czech Republic, belonging to the institution).
Edition Neues Jahrbuch für Geologie und Paläontologie, Stuttgart, 2016, 0077-7749.
Other information
Original language English
Type of outcome Article in a journal
Field of Study 10500 1.5. Earth and related environmental sciences
Country of publisher Germany
Confidentiality degree is not subject to a state or trade secret
Impact factor Impact factor: 0.777
RIV identification code RIV/00216224:14310/16:00089307
Organization unit Faculty of Science
Doi http://dx.doi.org/10.1127/njgpa/2016/0548
UT WoS 000370602600006
Keywords (in Czech) faciální analýza-provenience-foraminifery-vápnitý nannoplankton-dinoflagellata- pozice břežní čáry
Keywords in English facies analyses-provenance-foraminifera-calcareous nannoplankton-dinoflagellate cysts-shoreline position
Tags AKR, rivok
Changed by Changed by: prof. RNDr. Slavomír Nehyba, Dr., učo 2710. Changed: 13/3/2018 12:44.
Abstract
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.
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