The spatio-temporal patterns are used for the study of the intraplate seismicity of the Pannonian basin. The earthquake occurrence is connected to the strain rate values with the use of the Kostrov(1974) equation. It is shown that in the Pannonian basin the seismic rates are l0-7-l0-6. These values were derived from the local earthquake catalogues of the area of Komarom, Dunaharaszti (near Budapest) and Kecskemet. The method used in present study is based on combination of seismological and geodetic tools and it can be used in the future for the study of the seismic conditions of areas with reduced earthquake activity.
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