All

What are you looking for?

All
Projects
Results
Organizations

Quick search

  • Projects supported by TA ČR
  • Excellent projects
  • Projects with the highest public support
  • Current projects

Smart search

  • That is how I find a specific +word
  • That is how I leave the -word out of the results
  • “That is how I can find the whole phrase”

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

The result's identifiers

  • Result code in 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>

  • Alternative codes found

    RIV/00216224:14310/16:00089307

  • Result on the web

    <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>

Alternative languages

  • Result language

    angličtina

  • Original language name

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

  • Original language description

    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.

  • Czech name

  • Czech description

Classification

  • Type

    J<sub>x</sub> - Unclassified - Peer-reviewed scientific article (Jimp, Jsc and Jost)

  • CEP classification

    DB - Geology and mineralogy

  • OECD FORD branch

Result continuities

  • Project

  • Continuities

    I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Others

  • Publication year

    2016

  • Confidentiality

    S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Data specific for result type

  • Name of the periodical

    Neues Jahrbuch für Geologie und Palaontologie - Abhandlungen

  • ISSN

    0077-7749

  • e-ISSN

  • Volume of the periodical

    279

  • Issue of the periodical within the volume

    2

  • Country of publishing house

    DE - GERMANY

  • Number of pages

    30

  • Pages from-to

    209-238

  • UT code for WoS article

    000370602600006

  • EID of the result in the Scopus database

    2-s2.0-84996956158