GONDWANA RESEARCH, cilt.3, sa.3, ss.315-324, 2000 (SCI-Expanded)
The Lower Paleozoic rock-units in the Eastern Mediterranean can be separated into two distinct zones: the Northern Zone (Carpathian-Balkan, Istanbul, Zonguldak and Main Range terranes) acid the Southern Zone (Tauride-Anatolide, SE Anatolian-Arabian, and Central Iranian terranes). A Gondwanan /Perigondwanan origin can only be properly indicated for the Southern Zone, whereas the Early Paleozoic paleogeographic positions of smaller terranes (e.g. Istanbul Terrane) of the Northern Zone remains questionable.