. "3" . . "3"^^ . "Posp\u00ED\u0161il, Lubomil" . "RIV/00216305:26110/13:PU110012!RIV15-MSM-26110___" . "The Moravia territory has been the subject of geokinematic investigation within scope of several realized research projects and repeated GPS campaigns since 1992. The monitoring has been concentrated on all the Moravia region as well as on particular areas of interest concerning the eventual possible geodynamic changes (Kr\u00E1lick\u00FD Sn\u011B\u017En\u00EDk Massif, Diendorf-\u010Ceb\u00EDn Tectonic Zone (DCTZ) and others). At present time all the territory is covered by several tenths of permanent and epoch GNSS stations. Long observation time series at permanent stations alone are not sufficient for delivering the regional velocity field of sufficient density. On the other hand, epoch stations are more densely spread but periods of repeated observations are less frequent and often the data processing is not homogeneous. In the paper the preliminary kinematic model is briefly described which gives for the first time the general view of movement tendencies at the region of Moravia. On base of long-term monitoring it shows tha" . "3"^^ . . . . . "1214-9705" . "26110" . . "10" . . "CZ - \u010Cesk\u00E1 republika" . "15"^^ . . "Weigel, Josef" . "Movement tendencies in the Moravian region: Kinematical model"@en . . "RIV/00216305:26110/13:PU110012" . . . "89707" . "\u0160v\u00E1bensk\u00FD, Otakar" . . . "[3B6AA2EBC66C]" . "10.13168/AGG.2013.0030" . . . . "Movement tendencies in the Moravian region: Kinematical model" . "The Moravia territory has been the subject of geokinematic investigation within scope of several realized research projects and repeated GPS campaigns since 1992. The monitoring has been concentrated on all the Moravia region as well as on particular areas of interest concerning the eventual possible geodynamic changes (Kr\u00E1lick\u00FD Sn\u011B\u017En\u00EDk Massif, Diendorf-\u010Ceb\u00EDn Tectonic Zone (DCTZ) and others). At present time all the territory is covered by several tenths of permanent and epoch GNSS stations. Long observation time series at permanent stations alone are not sufficient for delivering the regional velocity field of sufficient density. On the other hand, epoch stations are more densely spread but periods of repeated observations are less frequent and often the data processing is not homogeneous. In the paper the preliminary kinematic model is briefly described which gives for the first time the general view of movement tendencies at the region of Moravia. On base of long-term monitoring it shows tha"@en . "Acta Geodynamica et Geomaterialia" . . "P(ED2.1.00/03.0097), S" . "Movement tendencies in the Moravian region: Kinematical model"@en . "Moravia, seismic hazards, GPS, geophysics, kinematic model"@en . . . "Movement tendencies in the Moravian region: Kinematical model" .