Geophysical Aspects of the Geotectonic Processes in the Vardar Zone and the Eastern Macedonian Zone

Abstract

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