The Ilovitsa porphyry Cu-Au deposit: Vein sequence, sulfide deposition and fluid inclusion study

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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