The Moho discontinuity was modelled on the basis of the 6 DSS profiles across the Yugoslav area, by the use of regression analysis and expressed by fitting surfaces from the 1st up to the 4th degree. Their characteristics were correlated to the geological structure of the Earth's crust, with intention to point out their connection with the deformations of the Moho discontinuity.
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Skoko et al. (1987) studied this question.
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