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	<meta name="DC.Creator.PersonalName" content="Gjorgi Dimov"/>
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	<div id="articleTitle"><h3>Geophysical Aspects of the Geotectonic Processes in the Vardar Zone and the Eastern Macedonian Zone</h3></div>
	<div id="authorString"><em>Blagica Doneva, Marjan Delipetrev, Gjorgi Dimov, Todor Delipetrov</em></div>
	<br />
			<div id="articleAbstract">
		<h4>Abstract</h4>
		<br />
		<div>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.</div>
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			<div id="articleCitations">
		<h4>References</h4>
		<br />
		<div>
							<p>Arsovski M., 1997: Tectonics of Macedonia, Faculty ofMining and Geology Štip</p>
							<p>Cimelzon I. A., Tkacuk I. Z., 1983: Mathematical Methodsfor Identification of Models in Geology, Moscow.</p>
							<p>Delipetrov T., Petrov G., 1990: Morphological-isostaticalcorrelation of the Debar – Kriva Palanka cross-section, XIIYugoslav geological congress, Ohrid</p>
							<p>Delipetrov T., 1991: Correlation between crusts and subcrustsstructures of the territory of Macedonia and seismicity,Doctor thesis, Faculty of Mining and Geology,Štip.</p>
							<p>Dragašević T., Andrić B., 1982: Results of investigationsof Earth's crust composition with deep seismic sounding inYugoslavia, Skopje.</p>
							<p>Golcman M. F., 1981: Statistic Interpretation of GeophysicalData, Leningrad.</p>
							<p>Interpreter of gravimetric map of the Republic of Macedonia– Bouguer anomalies – 1 : 500 000, Belgrade, 1976.</p>
					</div>
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