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P252 TIME SAG ANOMALIES VALIDATION BY MEANS OF THE P-P AND P-S SEISMIC DATA COMPARISON – THE CARPATHIAN FOREDEEP CASE Fig.1 The Carpathian Foredeep and the surrounding geological units. 1 The Carpathian Foredeep (CF) is the peripheral sedimentary foreland basin of the Alpine-age tectonic system created in relation to the moving Carpathians. It is extended along the Carpathian arc from Slovakia through Poland west-southern Ukraine to Romania. The big part of the foredeep covering about 18 000 km 2 is located in southern Poland. Fig.1 The hydrocarbon exploration was started here soon after the Second World War and during last