CARBON AND OXYGEN ISOTOPE SIGNATURE OF HYDROTHERMAL MINERAL DEPOSITS IN A POST-COLLISIONAL MAGMATIC-HYDROTHERMAL SYSTEM:  A REVIEW FROM NORTH MACEDONIA

Sabina  Strmić Palinkaš; Ladislav  Palinkaš; Goran Tasev; Dalibor  Serafimovski; Blažo  Boev

doi:10.46763/GEOL2539105sp

Sabina Strmić Palinkaš UiT The Arctic University of Norway, Faculty of Sciences and Technology, Department of Geosciences, Dramsvegen 201, N-9037 Tromsø, Norway
Ladislav Palinkaš University of Zagreb, Faculty of Science, Department of Geology, Horvatovac 95, HR-10000 Zagreb, Croatia
Goran Tasev Goce Delcev University, Faculty of Natural and Technical Sciences, Goce Delčev 89, MK-2000 Štip, North Macedonia
Dalibor Serafimovski Goce Delcev University, Faculty of Electrical Engineering, Goce Delčev 89, MK-2000 Štip, North Macedonia
Blažo Boev Goce Delcev University, Faculty of Natural and Technical Sciences, Goce Delčev 89, MK-2000 Štip, North Macedonia

DOI: https://doi.org/10.46763/GEOL2539105sp

Keywords: carbon; oxygen; isotope; hydrothermal; North Macedonia

Abstract

The subaerial magmatic-hydrothermal system exposed on the territory of Republic of North Macedonia represents a natural laboratory for studies of ore-forming processes associated with post-collisional magmatism. In this part of the Balkan Peninsula, neotectonics uplifted and exposed Tertiary post-collisional mineral deposits formed at different crustal levels, including deeply sitting porphyry Cu deposits, proximal and distal skarn deposits, and Carlin-like deposits. Locally epithermal deposits are also preserved. This paper summarizes and discusses previously published carbon and oxygen isotope data obtained from gangue carbonates collected from the key deposits in North Macedonia.

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