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Electrical conductivity inhomogeneities in Greece on the west margin of the Anatolian Fault

Ernst T.

Acta Geophysica Polonica

2005

Vol. 53, nr 1

103-114

Qualitative interpretation of the magnetotelluric results, based on the calculated polar diagrams and impedance tensors, is presented. The experimental data have been collected in Sterea Ellas region in Greece. Our interpretation allowed us to localize two conductive faults in the study area. One of them is probably a continuation of the west margin of the well-known Anatolian Fault.

Comments on the transmission of electric signals in dielectric media

Sarlis N., Varotsos P.

Acta Geophysica Polonica

2001

Vol. 49, nr 3

277-285

Recent findings indicate that the maximum horizontal principal stress s1 has a significant component perpendicular to the fault. This, upon assuming that the direction of s1 coincides with the dipole moment of the emitting source, is combined with "overamplification" phenomenon discussed recently. The numerical results strengthen the model suggested for the explanation of the "selectivity effect" of the Seismic Electric Signals.