Geophysical aspects of the geotectonic processes in the Vardar zone and the Eastern Macedonian zone

The paper deals with correlation dependencies of individual parameters of the Earth's crust in rela¬tion to the depth of Moho-discontinuity. These model investigations used data about the territory of the Republic of Mace¬donia. In the models, the territory was divided in three zones based on its neotectonic geologic setting [1]. The analysis carried out for the correlation coefficients for individual zones made possible the separation of zones relative to one another.