MICRO-SEISMIC MONITORING OF SEISMOGENIC ZONES IN HUNGARY

Abstract

RACT Hungary, or as geographically often referred the "Pannonian Basin" is situated in the territory between the Mediterranean area, which is seismically one of the active regions in the world, and the East European Platform which can be treated as nearly aseismic. In such seismically moderately active areas it really has been very chal­lenging to fmd correlation between known tectonic structures and earthquakes just using historical and early instrumental data. [...]