Podrobnosti záznamu

Název
    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)
Autor
    Hanžl, Pavel
    Hubatka, F.
    Krejčí, Oldřich
    Sedlák, Jiří
    Švancara, J.
Jazyk
    anglicky
Typ dokumentu
    část monografie (kapitola)
Rok
    2002
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
    Alpine
    Brittle
    Bruno-Vistulicum
    Carpathians
    Cover
    Czech
    Deformation
    Footwall
    Hercynian
    Outer
    Republic
    Sedimentary
    Units
    Western
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.
Přispěvatel
    Česká geologická služba
Kód přispěvatele
    ČGS (RIV)
Zdrojový formát
    R
Datum importu
    15. 10. 2014