Major Alpine Structures and Cu-Porphyry Mineralization in the Serbo-Macedonian Massif

Serafimovski, Todor and Tasev, Goran and Blažev, Krsto and Volkov, A. (2010) Major Alpine Structures and Cu-Porphyry Mineralization in the Serbo-Macedonian Massif. Geologica Macedonica, 24 (1). pp. 39-48. ISSN O352-1206

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Abstract

The geodynamic evolution of the Serbo-Macedonian massif can be reviewed in few geological
and geotectonic epochs, but very specific is the Cenozoic evolution from geodynamic, geotectonic, structural, magmatism
and metallogenetic point of view. The Cenozoic longitudinal structures are deep in their origin and represent
a boundary to the Vardar Zone on the one side and Struma Zone on the other side. Morphostructural forms of different
rank and intensity are of high importance for the spatial distribution of the ore mineralization (Kratovo-Zletovo
Pb-Zn-Cu ore district, Bucim-Damjan Cu-Au-Fe ore district, Bukovik-Kadiica Cu-Au-Ag-Fe ore system etc.). Predominant
structures within the Serbo-Macedonian massif are those with NW-SE direction, which served as orebearing
systems too (ore zone Besna Kobila-Osogovo-Tasos and metallogenetic zone Lece-Chalkidiki).

Item Type:	Article
Subjects:	Natural sciences > Earth and related environmental sciences
Divisions:	Faculty of Natural and Technical Sciences
Depositing User:	Goran Tasev
Date Deposited:	21 Nov 2012 19:14
Last Modified:	04 Jun 2013 09:09
URI:	https://eprints.ugd.edu.mk/id/eprint/1579

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