Paleotectonic-magmatic processe aiding mineralisation in the Carpatho-Balkanides of Eastern Serbia
Paleotektonsko-magmatski procesi kao preduslovi mineeralizacije u Karpato-Balkanidima Istočne Srbije
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.
Published
1995-12-20
How to Cite
Nikolić, P. and Đorđević, S. (1995) “Paleotectonic-magmatic processe aiding mineralisation in the Carpatho-Balkanides of Eastern Serbia”, Geološki anali Balkanskoga poluostrva, 59(1), pp. 53-76. Available at: https://gabp.rgf.rs/index.php/gabp/article/view/502 (Accessed: 9October2025).
Section
Original Scientific Paper
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