Dijapirizam kiselih plutona u Vardarskoj zoni

Acid pluton diapirism in the Vardar zone

  • Ilija Djoković University of Belgrade, Faculty of Mining and Geology, Institute of Regional Geology and Paleontology, Kamenička 6, 11000 Belgrade
  • Milun Marović University of Belgrade, Faculty of Mining and Geology, Institute of Regional Geology and Paleontology, Kamenička 6, 11000 Belgrade
  • Luka Pešić University of Belgrade, Faculty of Mining and Geology, Institute of Regional Geology and Paleontology, Kamenička 6, 11000 Belgrade
  • Branislav Trivić University of Belgrade, Faculty of Mining and Geology, Institute of Regional Geology and Paleontology, Kamenička 6, 11000 Belgrade
  • Marinko Toljić University of Belgrade, Faculty of Mining and Geology, Institute of Regional Geology and Paleontology, Kamenička 6, 11000 Belgrade
Keywords: Pluton, intrusion, diapirsm, dome

Abstract

Information about a very complex mechanism of granitoid plutonic body intrusion has been obtained through neotectonic and structurologic investigations of their bodies in the Vardar zone. The notably polykinetic occurrence is produced first by a classical intrusion, and later by diapiric piercing of solidified plutonic massifs. Diapirism is mainly recognized in Palaeozoic schists pierced by plutons, which have homotactic concordant fabric.

 

Published
1997-12-19
How to Cite
Djoković, I., Marović, M., Pešić, L., Trivić, B. and Toljić, M. (1997) “Dijapirizam kiselih plutona u Vardarskoj zoni”, Geološki anali Balkanskoga poluostrva, 61(1), pp. 17-26. Available at: https://gabp.rgf.rs/index.php/gabp/article/view/389 (Accessed: 22December2024).
Issue
Vol 61 No 1 (1997): Geološki anali Balkanskoga poluostrva
Section
Original Scientific Paper

Copyright (c) 1997 Geološki anali Balkanskoga poluostrva

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