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

  • Blagica Doneva
  • Marjan Delipetrev
  • Gjorgi Dimov
  • Todor Delipetrov

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.

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References

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.

Published
2013-09-25
How to Cite
Doneva, B., Delipetrev, M., Dimov, G., & Delipetrov, T. (2013). Geophysical Aspects of the Geotectonic Processes in the Vardar Zone and the Eastern Macedonian Zone. Geologica Macedonica, 26(1), pp.53–63. Retrieved from https://js.ugd.edu.mk/index.php/GEOLMAC/article/view/649