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

Local geology along the Sozina watersupply tunnel

  • 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.

Published
1995-12-20
How to Cite
Mirković, M. (1995) “Geološki sastav terena duž iskopa vodovodnog tunela ’’Sozina’’”, Geološki anali Balkanskoga poluostrva, 59(2), pp. 45-59. Available at: https://gabp.rgf.bg.ac.rs/index.php/gabp/article/view/456 (Accessed: 23November2024).
Issue
Vol 59 No 2 (1995): Geološki anali Balkanskoga poluostrva
Section
Original Scientific Paper

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