Neotektonska aktivnost šireg područja ''transverzale Skadar-Peć''

Neotectonic activity of the Scutari-Peć general area

Abstract

The border area of the Dinarides (s.str.) and the Hellenides, often termed "Scutari-Peć Transverse", has a complex fabric resulting from a staged sculpturing. The "Scutari-Peć Transverse" has been a conspicuous boundary between the Dinarides (s.str.) and the Hellenides since it was a part of Kimmerian framework. During the neotectonic deformations, it still has had a controlling part in structural relations. Available geological, geophysicaI and geomorphological documents and data have been used in defining the neotectonic activity of the ''Scutari-Peć Transverse" general area, establishing the mechanisms of movements, separating a number of neotectonic structures and faults, and defining their kinematic characters.