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

Blagica Doneva, Marjan Delipetrev, Gjorgi Dimov, Todor Delipetrov


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.


Arsovski M., 1997: Tectonics of Macedonia, Faculty ofMining and Geology Štip

Cimelzon I. A., Tkacuk I. Z., 1983: Mathematical Methodsfor Identification of Models in Geology, Moscow.

Delipetrov T., Petrov G., 1990: Morphological-isostaticalcorrelation of the Debar – Kriva Palanka cross-section, XIIYugoslav geological congress, Ohrid

Delipetrov T., 1991: Correlation between crusts and subcrustsstructures of the territory of Macedonia and seismicity,Doctor thesis, Faculty of Mining and Geology,Štip.

Dragašević T., Andrić B., 1982: Results of investigationsof Earth's crust composition with deep seismic sounding inYugoslavia, Skopje.

Golcman M. F., 1981: Statistic Interpretation of GeophysicalData, Leningrad.

Interpreter of gravimetric map of the Republic of Macedonia– Bouguer anomalies – 1 : 500 000, Belgrade, 1976.

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