Podrobnosti záznamu

    Hercynian and Alpine brittle deformation of the Bruno-Vistulicum and its sedimentary cover units in the footwall of the Outer Western Carpathians (E part of the Czech republic)
    Hanžl, Pavel
    Hubatka, F.
    Krejčí, Oldřich
    Sedlák, Jiří
    Švancara, J.
Typ dokumentu
    část monografie (kapitola)
Zdrojový dokument - monografie
    Krystalinikum, Contributions to the Geology and Petrology of Crystalline Complexes
Výraz tezauru
    Bruno-Vistulicum, Western Carpathians, Outer Flysch Belt, Carpathian Foredeep, Hercynian and Alpine orogenies, strucrural geology, thrust and nappe tectonics, thin skinned structures
Klíčové slovo
Abstrakt (anglicky)
   The deepest structural level and simultaneously the foreland of the Outer Western carpathians consist of the Bruno-Vistulian promontory of the Fenosarmatian Platform.During the Hercynian orogeny, when complicated, mainly nappe geological structure, was formed, was the Cadomian Bruno-Vistulic block with Paleozoic, Mesozoic and Tertiary platform sediments strongly affected by brittle thrust and nappe tectonic.This platform fundament was during the Alpine orogeny affected by brittle thrusting and strike-slip tectonic movements. However, the extent of the movements has not been properly clarified yet.
    Česká geologická služba
Kód přispěvatele
    ČGS (RIV)
Zdrojový formát
Datum importu
    15. 10. 2014