Geološki sastav terena duž iskopa vodovodnog tunela ''Sozina''

Local geology along the Sozina watersupply tunnel

Authors

  • Mirko Mirković Institute of Geological Investigations of the Republic of Montenegro, Krušenac bb, Podgorica, Montenegro.

Keywords:

Montenegro, Sozina, tunnels, Budva Zone, High Karst, pelagical Mesozoic

Abstract

This work presents results of the biostratigraphical field investigations of deposits exposed in the Sozina watersupply tunnel. The deposits through the length of the tunnel are Anisian sediments, Ladinian volcanogenic-sedimentary formation, Upper Triassic, Lower, Middle and Upper Jurassic, Cretaceous, and Paleogene sediments. All deposits form parts of two structural-facial units: High Karst and Budva Zone, in a tectonic relationship. The tunnel construction began in 1987 and was completed in April 1993.

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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

“Geološki sastav terena duž iskopa vodovodnog tunela ’’Sozina’’: Local geology along the Sozina watersupply tunnel” (1995) Geološki anali Balkanskoga poluostrva, 59(2), pp. 45–59. Available at: https://gabp.rgf.bg.ac.rs/index.php/gabp/article/view/456 (Accessed: 3 November 2026).