Abstract
A telluric station was installed on Crete in the South Aegean in order to investigate the existence of transient electric variations before large near intermediate-depth earthquakes.During the experiment, two transient electric variations (not correlated with geomagnetic variations) were recorded and associated with two time isolated intermediate-depth earthquakes with local magnitude ML 5.8 and 4.8, respectively.Finally a qualitative discussion on the form of the electric signal, based on the charge dislocation model, is presented.
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