Record details

Title
    Geodynamická evoluce krymsko-černomořské oblasti
Statement of responsibility
    Jan Prášek
Other titles
    Geodynamic evolution of the Crimean-Black sea region
Author
    Prášek, Jan
Language
    česky
Source title - monograph
    Současný stav geomorfologických výzkumů
Pages
    s. 62-69
Notes
    2 obr.
    Anglické resumé
    il.
    Obsahuje bibliografické odkazy
Subject group
    kenozoikum
    mesozoikum
    neotektonika
    tektonika desková
    Tethys
    vrásnění alpinské
    zemětřesení
Geographical name
    Černé moře
    Evropa jižní
    Turecko
    Ukrajina
Keyword
    Evoluce
    Geodynamická
    Krymsko-černomořské
    Oblasti
Abstract (in english)
   The new geodynamic model of Crimean-Black sea region was drawn up. This model is found on the principles of the new global tectonics theory. The paleozoic plates (euro-asian, afro-arabian and skythian) are base associated with microcontinents (Rodopia, Moesia, Crymia, Kavkazia, Dzirulia, Small Kavkazia, Sakaria, Eastern Anatolia, Kirschechiria and Menderesia) see fig. 2. The Crimean continent was formed during finish of paleozoic period in the beginning (see fig. 1). In the present, kvazisubduction of oceanic crust of Black sea under Crimean mountains is continued. Quaternary period is characteristic by intenzity of vertical movements, seismicity, tectonics activity and high intenzity of denudation processes
Contributor
    Česká geologická služba
Contributor code
    ČGS (UNM)
Source format
    U
Entered date
    18. 4. 2007
Import date
    8. 8. 2012