Paleotectonic-magmatic processe aiding mineralisation in the Carpatho-Balkanides of Eastern Serbia

Paleotektonsko-magmatski procesi kao preduslovi mineeralizacije u Karpato-Balkanidima Istočne Srbije

Authors

  • Predrag Nikolić University of Belgrade, Faculty of Mining and Geology,Institute of Regional Geology and Paleontology, Kamenička 6, 11000 Belgrade, Serbia.
  • Slobodan Đorđević Engineering Faculty of Bor, 19210 Bor, Serbia.

Keywords:

Tectonic cycles, magmatism and mineralisation, type of deposits, hydrothermal processe, metallic mineralisation

Abstract

The interrelation and association of tectonic and magmatic processes in the Carpatho-Balkanides of eastern Serbia are responsible for numerous mineralisations, and significant metallic ore deposits. Tectono-magmatic processes in this part of Serbia began as early as in the Precambrian and continued through several divisions to the present state of the lithospheric evolution. The most important was the Alpine tectono-magmatic cycle, lead-zinc and other minerals were formed.

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Published

1995-12-20

Issue

Vol. 59 No. 1 (1995): Geološki anali Balkanskoga poluostrva

Section

Original Scientific Paper

How to Cite

“Paleotectonic-magmatic processe aiding mineralisation in the Carpatho-Balkanides of Eastern Serbia: Paleotektonsko-magmatski procesi kao preduslovi mineeralizacije u Karpato-Balkanidima Istočne Srbije” (1995) Geološki anali Balkanskoga poluostrva, 59(1), pp. 53–76. Available at: https://gabp.rgf.bg.ac.rs/index.php/gabp/article/view/502 (Accessed: 4 November 2026).