The article presents results of paleomagnetic investigation of the NW part of the Pannonian Basin. More than 170 independently oriented sedimentary samples from 10 localities from Hungarian and Slovak side were subjected to the AF and thermal demagnetization. They were sandstones, siltstones, marls and limestones and their age is late Cretaceous -late Miocene. The results gave counterclockwise rotation with angles of declination between an important common component to the Cenozoic movements affecting the present NW part of the Pannonian Basin.