Abstract
The Dinarides, the Eastern Alps and the Western Carpathians being situated at the borders of the Pannonian basin, are of very similar origin. Therefore, the results obtained in the investigation of correlations between Earth gravity field parameters (absolute geoid undulations, gravity anomalies), the surface topography and the shape of the Mohorovičić discontinuity, were compared. It was found that these three regions have the same basic characteristics, but also their own specific features. While the similarities follow clearly from these investigations, the found differences might partly be a consequence of non-uniformity and unmatched quality of data sets used for the three regions.
Original language | English |
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Pages (from-to) | 131-139 |
Number of pages | 9 |
Journal | Studia Geophysica et Geodaetica |
Volume | 38 |
Issue number | 2 |
DOIs | |
Publication status | Published - 1 Apr 1994 |
ASJC Scopus subject areas
- Geophysics
- Geochemistry and Petrology