Seismotectonically Active Zones in the Dinarides
Seismotectonically active zones are formed due to displacements of segments of the Adriatic micro-plate that differ in size and in their rate of movement, and by the resistance of the rock masses of the Dinarides. The spatial position of these zones can be determined through the locations of earthqu...
| Main Authors: | , , |
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| Format: | Article |
| Language: | English |
| Published: |
Croatian Geological Survey
2000-12-01
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| Series: | Geologia Croatica |
| Subjects: | |
| Online Access: | http://www.geologia-croatica.hr/ojs/index.php/GC/article/view/260 |