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

Neotectonic activity of the Scutari-Peć general area

Authors

  • Milun Marović University of Belgrade, Faculty of Mining and Geology, Đušina 7, 11000 Belgrade, Serbia.
  • Ilija Đoković University of Belgrade, Faculty of Mining and Geology, Đušina 7, 11000 Belgrade, Serbia.

Keywords:

Neotectonics, Scutari-Peć Transverse, mechanisms of neotectonic movements, neotectonic structures and faults

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.

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Published

1995-12-20

Issue

Vol. 59 No. 2 (1995): Geološki anali Balkanskoga poluostrva

Section

Original Scientific Paper

How to Cite

“Neotektonska aktivnost šireg područja ’’transverzale Skadar-Peć’’: Neotectonic activity of the Scutari-Peć general area” (1995) Geološki anali Balkanskoga poluostrva, 59(2), pp. 23–43. Available at: https://gabp.rgf.bg.ac.rs/index.php/gabp/article/view/455 (Accessed: 3 November 2026).