Peytcheva, Irena and Grozdev, Valentin and Georgiev, Stoyan and von Quadt, Albrecht and Marchev, Peter and Serafimovski, Todor and Tasev, Goran (2014) Cenozoic magmatism in the border area of W Bulgaria - E Macedonia - SE Serbia: temporal evolution, geochemical trends and fertility in changing compression-extension regime. Proceedings of the XX Congress of Carpathian Balkan Geological Association, Special Issue, 1 (1). p. 176. ISSN 0254-5276; 2306-9600
Preview |
Text
Peytcheva et al CBGA 2014 Tirana complete.pdf Download (1MB) | Preview |
Abstract
The Balkan Peninsula is one of Europe's
mineralized regions with world-class ore deposits.
Numerous porphyry Cu-(Au-Mo) and epithermal
Au-(Cu) deposits are related to Upper Cretaceous
calc-alkaline magmatism formed during oblique
northward subduction of the Tethys beneath the
European continent and slab roll-back. The next
time period with important Pb-Zn-Au-Cu
mineralization is Cenozoic (mainly Oligocene) and
related to post-collisional magmatism. We present
here integrated U-Pb zircon, Sr-Nd-Hf isotope and
geochemical analyses on Palaeogene rocks from W
Bulgaria, SE Serbia and E Macedonia (FYROM)
with the aim to constrain the temporal and tectonomagmatic evolution of the region that favoured
significant ore-formation.
Item Type: | Article |
---|---|
Subjects: | Natural sciences > Earth and related environmental sciences |
Divisions: | Faculty of Natural and Technical Sciences |
Depositing User: | Goran Tasev |
Date Deposited: | 03 Oct 2014 08:07 |
Last Modified: | 03 Oct 2014 08:07 |
URI: | https://eprints.ugd.edu.mk/id/eprint/11060 |
Actions (login required)
View Item |