Au-Pd AND Bi-Se BEARING PYRITE AND CHALCOPYRITE FROM THE BUCHIM COPPER MINE, EASTERN MACEDONIA

  • Todor Serafimovski University "Goce Delcev"- Stip, Faculty of Natural and Technical Sciences, Institute of Geology, str. Bul. Goce Delcev No.89, 2000 Stip, Republic North Macedonia
  • Tadej Dolenec Department of Geology, Faculty of Natural Sciences and Engineering, University of Ljubljana, Aškerčeva 12, 1000 Ljubljana, Slovenija
  • Goran Tasev University "Goce Delcev"- Stip, Faculty of Natural and Technical Sciences, Institute of Geology, str. Bul. Goce Delcev No.89, 2000 Stip, Republic North Macedonia
  • Dalibor Serafimovski University "Goce Delcev"- Stip, Faculty of Natural and Technical Sciences, Institute of Geology, str. Bul. Goce Delcev No.89, 2000 Stip, Republic North Macedonia
  • Nastja Rogan Šmuc Department of Geology, Faculty of Natural Sciences and Engineering, University of Ljubljana, Aškerčeva 12, 1000 Ljubljana, Slovenija
  • Matej Dolenec Department of Geology, Faculty of Natural Sciences and Engineering, University of Ljubljana, Aškerčeva 12, 1000 Ljubljana, Slovenija
Keywords: ore minerals, Au-Pd phases, rare Bi-Se mineral phases, Buchim mine

Abstract

In the Buchim porphyry copper deposit, we determined several representative rare mineral phases, comprising metals from the gold-palladium group as well as those from the bismuth-selenium (Cu-Bi-Se-Te-As) group. The bismuth-selenium rare mineral phases are represented by new rare mineral phases in the Buchim porphyry copper deposit, bismuthinite, galenobismutite, krupkaite, friedrichite, emplectite, laitakarite and native bismuth as well as mineral phases of gold-palladium, including gold and palladium with their elemental mixtures. It should be stressed that both types of rare mineral phases were determined in pyrite and chalcopyrite from major ore paragenesis in the Buchim deposit. The bismuth-selenium mineral phases were related to the major quartz-pyrite-chalcopyrite paragenesis, while the gold-palladium phases were related to a slightly higher temperature, oxido-sulphide parageneses such are magnetite-pyrite-chalcopyrite (Mt-Py-Cp) and pyrite-chalcopyrite (Py-Cp).

References

1 T. Serafimovski, V. Cifliganec, S. Jankovic, B. Boev, Genetic Model of the Buchim Porphyry Copper Deposit, Republic of Macedonia, Proceedings of the Annual Meeting, UNESCO-IGCP Project 356, Vol. 1, Sofija 1996, 63–75
2 V. Čifliganec, Copper Mineralization in the Republic of Macedonia, 1st ed., Universitet "Sv. Kiril i Metodij", Skopje 1993, 303
3 M. Pavičević, S. Rakić, Study of occurence of gold, silver and other rare elements in ores from the Central ore body, Buchim, ULEMA, Belgrade 1983, 202
4 T. Serafimovski, G. Tasev, P. Lazarov, Au-Ag-Te-Bi-Se minerals associated with porphyry copper mineralization in the Buchim copper mine, R. Macedonia. Au-Ag-Te-Se depo¬s¬i¬ts IGCP-486, Field Workshop, Izmir 2006, 154–158
5 R. Petrunov, T. Serafimovski, P. Dragov, New finding of PGE-mineralisation in porphyry-copper environment-the Buchim deposit, Macedonia: preliminary microscope and microprobe data, ABCD-GEODE 2001 Workshop Vata Bai, Romania 2001, 79–80
6 S. Janković, Ore deposit of Serbia, Faculty of Mining and Geology, Belgrade 1990, 765
7 M. Tarkian, D. G. Eliopoulos, M. Economou-Eliopoulos, Mineralogy of precious metals in the Skouries porphyry copper deposit, N. Greece, Neues Jahrbuch fur Mineralogie Abhandlungen, 1991, 529–537
8 R. Petrunov, P. Dragov, G. Ignatov, H. Heykov, Ts. Iliev, N. Vassileva, V. Tzatzov, S. Djunakov, K. Doncheva, Hydrothermal PGE-mineralization in the Elatsite porphyry-copper deposit (Sredna Gora metallogenic zone, Bulgaria), Comptes Rendu Academie Bulg. Sci, 45/4 (1992) 37–40
9 M. Economou-Eliopoulos, Platinum-group elements (PGE) in various geotectonic settings: Opportunities and risks, Hellenic Journal of Geosciences, 45 (2010) 65–82
10 C. P. Voudouris, G. P. Spry, C. Mavrogonatos, G. A. Sakellaris, K. S. Bristol, V. Melfos, P. A. Fornadel, Bismuthinite derivatives, lillianite homologues, and bismuth sulfotellurides as indicators of gold mineralization in the Stanos shear-zone related deposit, Chalkidiki, Northern Greece, The Canadian Mineralogist, 51 (2013), 119–142, doi:10.3749/canmin.51.1.119
11 T. Serafimovski, Structural-metallogenic features of the Lece-Chal¬kidiki zone: types of mineral deposit and distribution. Special Issue No. 2. University of St Cyril and Methodius, Stip 1993, 325
12 V. A. Volkov, T. Serafimovski, V. Stefanova, A. A. Sidorov, Formation Mechanism of Dwarfish Cu–Au Porphyry Deposits of Macedonia, Doklady Earth Sciences, 431/2 (2010), 429–434
13 K. Pockov, Geochemical types of pyrites in the porphyry copper deposit Buchim. Master thesis, Faculty of Mining and Geology, Štip 1997, 125
14 G. Tasev, T. Serafimovski, REE in some Tertiary volcanic complexes in the Republic of Macedonia. Geologica Macedonica, 23 (2009), 17–25
15 S. Lehmann, J. Barcikowski, A. von Quadt, D. Gallhofer, I. Peytcheva, C. A. Heinrich, T. Serafimovski, Geochronology, geochemistry and isotope tracing of the Oligocene magmatism of the Buchim-Damjan-Borov Dol ore district: Implications for timing, duration and source of the magmatism, Lithos, 180–181 (2013), 216–233
16 M. Kolb, A. von Quadt, I. Peytcheva, C. A. Heinrich, S. J. Fowler, V. Cvetkovic, Adakite-like and normal arc magmas: distinct fractionation paths in the East Serbian segment of the Balkan–Carpathian Arc. Journal of Petrology 1–31 (2012), doi:10.1093/petrology/ egs072
17 M. Economou-Eliopoulos, G. D. Eliopoulos, Palladium, platinum and gold concentration in porphyry copper systems of Greece and their genetic significance. Ore Geology Reviews, 16 (2000) 59–70
18 P. Frei, Evolution of mineralizing fluid in the porphyry copper system of the Skouries deposit, northeast Chalkidiki -Greece: evidence from combined Pb–Sr and stable isotope data,Econ. Geol. 90 (1995), 746–762
Published
2021-03-16
How to Cite
1.
Serafimovski T, Dolenec T, Tasev G, Serafimovski D, Rogan ŠmucN, Dolenec M. Au-Pd AND Bi-Se BEARING PYRITE AND CHALCOPYRITE FROM THE BUCHIM COPPER MINE, EASTERN MACEDONIA. MatTech [Internet]. 2021Mar.16 [cited 2026Sep.8];55(1):71-6. Available from: https://mater-tehnol.si/index.php/MatTech/article/view/107