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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.

GEOPHYSICAL ASPECTS OF THE GEOTECTONIC PROCESSES IN THE VARDAR ZONE AND THE EASTERN MACEDONIAN ZONE