Podrobnosti záznamu

Název
    Brunovistulian terrane (Czech Republic, Middle European Variscides) and Lower Carboniferous Paleobiogeography
Autor
    Kalvoda, Jiří
Jazyk
    anglicky
Typ dokumentu
    článek ve sborníku
Zdrojový dokument - monografie
    I COngresso Ibérico de Paléontología, XVI Jornadas de la Sociedad Espanola de Paleontologia, Livro de Resumos
Strany
    1
Poznámky
    Akce: 2000 ; 12-14. 10. 2000, Evora
Výraz tezauru
    Brunovistulian terrane
    Lower Carboniferous
    paleobiogeography
Klíčové slovo
    Brunovistulian
    Carboniferous
    Czech
    European
    Lower
    Middle
    Paleobiogeography
    Republic
    Terrane
    Variscides
Abstrakt (anglicky)
   The Brunovistulian Terrane was similarly as the Eastern Avalonia Terrane a part of the Panafrican (Cadomian) Gondwana margin. The lithological record of the Cambrian marine sediments may indicate the extension and rifting connected with the fragmentation of Gondwana while the faunistic record of Cambrian fauna shows close relation to Baltica (Belka et al. 1999). It is assumed that the Brunovistulian Terrane was amalgamated to the southeastern margin of Baltica and dextral translation is characteristic for its contact with northern Malopolska Terrane along the Krakow-Lubliniec Zone (Grygar, Vavro 1995). Thus the Brunovistulian Terrane was amalgamated to Baltica similarly as the Eastern Avalonia Terrane in the Lower Paleozoic, however, the Eastern Avalonian Terrane shows, contrary to the Brunovistulian Terrane, predominant sinistral translation. This differencies between the eastern and western part of the Middle European Variscides may have continued in the Upper Paleozoic.
Přispěvatel
    MU Brno, Přírodovědecká fakulta
Kód přispěvatele
    MU, PřF
Zdrojový formát
    R
Datum importu
    8. 8. 2012