Podrobnosti záznamu

Název
    Brunovistulian Terrane (Central Europe) and Istanbul Zone (NW Turkey): Late Proterozoic and Paleozoic tectonostratigraphic development and paleogeography
Autor
    Bábek, Ondřej
    Kalvoda, Jiří
    Leichmann, Jaromír
    Melichar, Rostislav
Jazyk
    anglicky
Typ dokumentu
    článek v periodiku
Zdrojový dokument - seriál
    Geologica Carpathica
Svazek/č.
    Roč. 54, č. 3
Strany
    13
Rok
    2003
Výraz tezauru
    : Brunovistulicum
    Istanbul Zone
    late Proterozoic
    paleogeography
    Paleozoic.
    terranes
Klíčové slovo
    Brunovistulian
    Central
    Development
    Europe
    Istanbul
    Late
    NW
    Paleogeography
    Paleozoic
    Proterozoic
    Tectonostratigraphic
    Terrane
    Turkey
    Zone
Abstrakt (anglicky)
   There are close similarities between the Brunovistulian Terrane and the Istanbul Zone both in the Neoproterozoic and Paleozoic. The geological structure, lithology and geochronology of the Cadomian Brunovistulicum show broad fit with the crystalline basement of the Istanbul Zone. Their Gondwana or Baltica affinity is still poorly constrained and remains a matter of discussion. The Vendian and Cambrian sequences recognized in central Malopolska, Brunovistulian and Moesian terranes correlate well with the Scythian Platform. In the Istanbul Zone the presence of the pre-Ordovician sedimentary sequences has not been confirmed and may be only anticipated. In Paleozoic the best fit was attained in the Devonian-Carboniferous interval.The sedimentary record in the Zonguldak and Istanbul terranes closely compares to the Moravian Karst and Ludmirov facies developments of the Brunovistulian Terrane.
Přispěvatel
    MU Brno, Přírodovědecká fakulta
Kód přispěvatele
    MU, PřF
Zdrojový formát
    R
Datum importu
    8. 8. 2012