The area of western border of the CEI member countries is created by different geological structures as a part of Easter Alps, Carpathians, Pannonian Basin, Bohemian Massif and eastern area of Polish platform. This area includes northern slopes of the Alps, their foredeep and contact with the Bohemian Massif, West Carpathians foredeep towards Bohemian Massif and a part of Polish platform, crossing area of Sudeten fault zone and T-T zone. The entire territory is covered by map of annual velocities of vertical movements as well as by network of GPS stations. In present paper the geodynamical properties of mentioned above territory are analysed and shortly discussed both in vertical and horizontal component. It should be added that the vertical movements are derived from repeated levelling performed before and after the World War II and 1995. The horizontal component is derived from satellite (GPS) measurements after 1994 (see Fig. 1).
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