The permanent GPS measurements bring independent effective phenomenon, direct monitoring of site movements. Knowledge of local physical processes based on spatial and time earthquake occurrences, focal mechanisms of main events, stress and strain fields set up a tool for recent seismotectonic analyses. Their mutual position changes were determined from time series of GPS observations and were associated with seismic, gravity, and geo-scientific data related to the geodynamics of the West Bohemian region. In West Bohemia in the period of 2003–2005 five permanent GPS stations were established to detect local movement trends.
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