| Popis: |
On the basis of the seismotectonic analysis we distinguish two deep fault zones of the crust: The Ionian-Adriatic fault zone and the zone of Shkodra depressional faults. The earthquake of April 15, 1979 was generated from the first deep fault zone of the crust that is located on the outer side of the orogene, of the Dinaride-Albanide-Hellenide branch of the folded alpine belt of the Mediterranean, at the border with the platform. The seismogene block activated during the earthquake was the under water Ulqin-Budva block with a length of 40 km. |
