Carboniferous foraminiferal paleobiogeography in Turkey and its implications for plate tectonic reconstructions

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Publikace nespadá pod Ekonomicko-správní fakultu, ale pod Přírodovědeckou fakultu. Oficiální stránka publikace je na webu muni.cz.
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KALVODA Jiří

Rok publikování 2003
Druh Článek v odborném periodiku
Časopis / Zdroj Rivista Italiana di Paleontologia e Stratigrafia
Fakulta / Pracoviště MU

Přírodovědecká fakulta

Citace
www http://www.gp.terra.unimi.it/rivista/rivista.html
Obor Geologie a mineralogie
Klíčová slova Istanbul Zone; Aladag Nappe; Anatolide-Tauride Zone; Laurussia
Popis 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. Later, in the Permian, the Anatolide -Tauride Zone may has been separated from the Eurasian mainland by the Karakaya back-arc ocean.
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