New insights on the geochemical affinity and age of mineralized rocks in Timok magmatic complex, East Serbia

Author:

Velojic Milos1ORCID,Klimentyeva Dina2,von Quadt3,Guillong Marcel3,Melcher Frank4,Meisel Thomas4,Prelevic Dejan1ORCID

Affiliation:

1. Faculty of Mining and Geology, Belgrade, Serbia

2. GoldSpot Discoveries Corp., Toronto, Canada

3. Department of Earth Sciences, ETH Zurich, Zurich, Switzerland

4. Montanuniversität Leoben, Leoben, Austria

Abstract

Bor and Cukaru Peki are world-class porphyry deposits spatially and genetically associated with the Cretaceous Timok magmatic complex. This research was conducted to determine the age and geochemical affinity of the magmatic rocks that formed these ore deposits. Our new geochemical analyses of magmatic rocks from Bor and Cukaru Peki deposits imply they comprise adakite-like compositions that have undergone the amphibole fractionation and sulphide saturation processes. The zircon ages indicate that the Bor system was formed in the age span between 84.5?82 Ma, while the Cukaru Peki system was created in the age span between 86.5?85 Ma.

Publisher

National Library of Serbia

Subject

Paleontology,Stratigraphy,Economic Geology,Geochemistry and Petrology,Geology,Geophysics,Geotechnical Engineering and Engineering Geology

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