Podrobnosti záznamu

Název
    Carboniferous foraminiferal paleobiogeography in Turkey and its implications for plate tectonic reconstructions
Autor
    Kalvoda, Jiří
Jazyk
    anglicky
Typ dokumentu
    článek v periodiku
Zdrojový dokument - seriál
    Rivista Italiana di Paleontologia e Stratigrafia
Svazek/č.
    Roč. 109, č. 2
Strany
    11
Rok
    2003
Výraz tezauru
    Aladag Nappe
    Anatolide-Tauride Zone
    Istanbul Zone
    Laurussia
Klíčové slovo
    Carboniferous
    Foraminiferal
    Implications
    Paleobiogeography
    Plate
    Reconstructions
    Tectonic
    Turkey
Abstrakt (anglicky)
   Four foraminiferal paleobiogeographic realms are distinguished in the Carboniferous - North Paleotethyan, Perigondwanian, Siberian and North American. The Carboniferous foraminiferal faunas of both the Istanbul and Anatolide-Tauride zones distinctly differ from both Cimmerian terranes (Central Afghanistan, Qiangtang) and Libya and Egypt of the Perigondwana Realm and show close relation to the North Paleotethyan Realm, especially to the Fennosarmatian Province of southeastern Laurussia (Moesian and Scythian platforms) or to the Central Asiatic Province. A model that best fits with available evidence is that the Anatolide-Tauride Zone was either a part or located close to Laurasia in Carboniferous. The Istanbul Zone represents an equivalent of the Rhehohercynian Zone of the Central Europe and can not be compared with Intra-Alpine or south Variscan terranes which may be correlated with the Anatolide-Tauride Zone.
Přispěvatel
    MU Brno, Přírodovědecká fakulta
Kód přispěvatele
    MU, PřF
Zdrojový formát
    R
Datum importu
    8. 8. 2012