Gosau Deposits of the Apuseni Mts. as a Support to Understanding the Geodynamic Evolution of the Alpine/Carpathian Orogen

plain environments (Fig. 2d). Paleotransport indicators in lower part of the Huty Fm. suggest to east northward to west northward oriented paleocurrents, reprendicular to basin axis. Sediments of Zuberec Fm., developed during Mid-Oligocene see level fall, they were deposited in elongate, more sand-rich fan (Fig. 2e). The study area is on distal part of this fan, however, shallow chan-nels flanked by levees often reached into smooth, outer fan area. Youngest preserved part of the CCPB fill represents deposit of Biely Potok Fm., which is typical sand-rich fan (Fig. 2f). Proxi-mal part of this fan with well developed suprafan lobes is in west-ern part of basin (Orava region), in study area is preserved its dis-tal part (Brzegi Mb.). Paleotransport direction in both, Zuberec Fm. and Brzegi Mb. is oriented toward east; submarine fans were redirected to axial position in basin. Reference