Podrobnosti záznamu

    Sedimentary architecture of the southern part of the Carpathian Foredeep.
    Nehyba, Slavomír
Typ dokumentu
    článek ve sborníku
Zdrojový dokument - monografie
    23rd IAS Meeting of Sedimentology - Abstract Book
    Akce: 2004 ; Coimbra, Portugalsko
Výraz tezauru
    Carpathian Foredeep
    sequence stratigraphy
Klíčové slovo
Abstrakt (anglicky)
   The Carpathian Foredeep is a peripheral foreland basin, formed by flexural downbuckling of the passive North European Plate (Bohemian Massif) in the foreland due to the loading of the Apine-Carpathian orogene belt. Southern part of the basin is filled by Neogene clastic deposits (Egerian to Lower Badenian i.e. 22,5 Ma-15,5 Ma). Shallow marine and coastal deposits strongly predominates (underfilled foreland basin). The sedimentary record of the basin was divided into genetically related depositional units, limited by key surfaces, and controlling factors of their sedimentation were defined. The study is based exclusively on subsurface data (drill cores, wireline logs, reflection seismic profiles). Five evolutional stages of the basin/3rd order depositional sequences were selected illustrating its dynamic evolution. Individual stages are typical by various basin shape, geometry, depositional architecture and character of the deposits, i.e.
    MU Brno, Přírodovědecká fakulta
Kód přispěvatele
    MU, PřF
Zdrojový formát
Datum importu
    8. 8. 2012