Stefanova, Elitsa and Georgiev, Stoyan and Peytcheva, Irena and Heinrich, Cristoph and von Quadt, Albrecht and Donkova, Aneta and Serafimovski, Todor (2014) The Ilovitsa porphyry Cu-Au deposit: Vein sequence, sulfide deposition and fluid inclusion study. Proceedings of the XX Congress of Carpathian Balkan Geological Association, Special Issue, 1 (1). p. 178. ISSN 0254-5276; 2306-9600
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Abstract
The Ilovitsa porphyry Cu-Au deposit is located 30 km
away from the town of Strumitsa, SE FYR
Macedonia. It is hosted in a Triassic granite (251.90
±0.89 Ma, Georgiev et al. 2013).The latter intrudes
into the metamorphic rocks of the Vertiscos-
Ograzhden Unit of the Serbo-Macedonian massif.
Formation of the Ilovitsa deposit is related to the
intrusion of multiple Tertiary porphyry intrusions
(called the Ilovitsa Stock) and dykes. The Ilovitsa
stock that hosts the Cu-Au mineralization is made up
by two main intrusions with a similar granodioritic
composition dated by ID-TIMS at 30.31 ±0.05 Ma
and 30.13±0.03 Ma (Georgiev et al. 2013). The
authors have determined that the ages of the dykes are
between 28.8 and 29.6 Ma.
| 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 08:03 |
| Last Modified: | 03 Oct 2014 08:03 |
| URI: | https://eprints.ugd.edu.mk/id/eprint/11059 |
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