The experimental study of the temperature-frequency dependence of permittiv
ity epsilon and dielectric loss tangent tan delta in igneous rocks of a com
plex dike in southern Daghestan is carried out at frequencies of 5 x 10(4)-
5 x 10(6) Hz and at temperatures of 20-900 degreesC. It is experimentally s
hown that epsilon increases exponentially with temperature above 400 degree
sC, and relaxation maximums are typically present in the curves tan delta =
f(T). Based on the results obtained, the activation energy of the relaxati
on process is calculated. The temperature dependence of e is found to be se
nsitive to the FeO concentration in granite-porphyry and diabase samples.