Majdanpek

Porphyry copper (Cu-Au) deposit in Bor, Serbia

Names and other identifiers

GMRAP ID 372
Tract name Transylvania-Balkan Mountains (150pCu6001)
Site status deposit

Geographic location

Country Serbia
State or province Bor
Geographic location 21.932355, 44.410826
Geologic map unit 21.932355, 44.410826
Nearby data

Geologic information

Deposit type Porphyry copper
Deposit subtype Cu-Au
Age (Ma) 83.6Ma
Age determination method Ar-Ar biotite, hornblende
Age range 83.6 to 84.0 ±0.6 Ma
Age reference Clark and Ulrich (2004)
Minerals arsenopyrite, biotite, bismuth, bornite, carbonates, chalcopyrite, chlorite, enargite, epidote, galena, gold, magnetite, marcasite, molybdenite, pyrite, pyrrhotite, selenides, sericite, sphalerite, stannite, tellurides, tetrahedrite/tennantite
Associated rocks andesite, monzodiorite porphyry, skarn, conglomerate, marl, monzodiorite, Incamphibolite, gneiss, limestone, phyllite
Tectonic setting continental margin
Stratigraphic age Late Cretaceous

Commodity and development information

Development status Producer
Major commodities Cu
Tonnage (Mt) 1,000Mt
Cu grade (%) 0.6%
Mo grade (%) 0.005%
Au grade (g/t) 0.35g/t
Ag grade (g/t) 1g/t
Contained copper 6,000,000t
Gold-Moly ratio 70

Reference information

Comments Porphyry copper-gold deposit with associated replacement deposits (skarns, mantos) and high-sulphidation epithermal massive-enargite (gold) sulphide deposits. The deposit was mined to 1962 for massive pyrite and limonite, but since then the large porphyry copper deposit was mined by open pit with an annual production of 12–14 Mt (Jelenkovi? and others, 2007). Reserves at Majdanpek are estimated at 800 Mt of ore, containing 0.4–0.8 % Cu, and 0.25–1.0 g/t Au (Jelenkovi? and others, 2007). In concentrate: 7.8 g/t Au, 0.03 g/t Pt, 0.27 g/t Pd. Exposed. Location is for center of pit lake on Google Earth image. The main mineralization stage at Majdanpek occurred at 83.6–84.0 ±0.6 Ma, coinciding with the later stages of the first cycle of high-potassium calc-alkaline andesitic volcanism in the district (Clark and Ullric, 2004). Drew (2005) shows the Majdanpek porphyry copper deposit occurs in Late Cretaceous andesite as part of a positive flower structure within the northern extension of a north-trending strike-slip fault duplex.
Study area name Europe
References Anonymous (1973a); Armstrong and others (2005); Clark (1993); Clark and Ulrich (2004); Drew (2006); Herrington and others (1998); Herrington and others (2003); Jankovi? (1982); Jankovi? and others (1980); Lips and others (2006); Jelenkovi? and others (2007); Monthel and others (2002); Starostin (1970); Tarkian and Stribrny (1999); Singer and others (2008)
Site reference Sutphin and others (2013)
Anonymous, 1973a, Majdanpek copper mine: Mining Magazine, September, p. 182–187.
Armstrong, R., Kozelj, D., and Herrington, R., 2005, The Majdanpek Cu-Au deposit of eastern Serbia, a review, in Porter, T.M., ed., Super porphyry copper and gold deposits—A global perspective: Adelaide, PGC Publishing, v. 2, p. 453–466. (Abstract also available at http://www.portergeo.com.au/publishing/superporphyry/superpstart.html.)
Clark, A.H., 1993, Are outsize porphyry copper deposits either anatomically or environmentally distinctive?, in Whiting, B.H., Hodgson, C.J., and Mason, R., eds., Giant ore deposits: Society of Economic Geologists Special Publication 2, p. 213–283.
Clark, A.H., and Ulrich, T.D., 2004, 40Ar-39Ar age data for andesitic magmatism and hydrothermal activity in the Timoc Massif, eastern Serbia–Implications for metallogenic relationships in the Bor copper-gold province: Mineralium Deposita, v. 39, p. 256–262. (Also available at http://dx.doi.org/10.1007/s00126-003-0370-3.)Drew, L.J., 2006, A tectonic model for the spatial occurrence of porphyry copper and polymetallic vein deposits—Applications to Central Europe: U.S. Geological Survey Scientific Investigations Report 2005–5272, 36 p. (Also available at http://pubs.usgs.gov/sir/2005/5272/.)Herrington, R.J., Jankovi?, S., and Kozelj, D., 1998, The Bor and Majdanpek copper-gold deposits in the context of the Bor metallogenic zone (Serbia, Yugoslavia), in Porter, T.M., ed., Porphyry and hydrothermal copper and gold deposits a global perspective: Adelaide, PGC Publishing, Australian Mineral Foundation International Conference, Perth, Western Australia, November 30–December 1, 1998 [Proceedings], p. 185–194. (Abstract also available at http://www.portergeo.com.au/publishing/porphyry98/porphyry98start.html.)
Herrington, R.J., First, D.M., and Kozelj, D., 2003, Copper porphyry deposits in Hungary, Serbia, Macedonia, Romania and Bulgaria, in Kelly, J.G., and others, eds., Europe’s major base metal deposits: Irish Association for Economic Geology (IAEG) Conference, Dublin, May 2000, p. 303–321.
Jankovi?, S., 1982, Yugoslavia, in Dunning, F.W., Mykura, W., and Slater, D., eds., Mineral deposits of Europe, Volume 2—Southeast Europe: London, The Institution of Mining and Metallurgy and the Mineralogical Society, p. 143–202.
Jankovi?, S., Terzic, M., Aleksic, D., Karamata, S., Spasov, T., Jovanovic, M., Milicic, M., Miscovic, V., Grubic, A., and Antonijevich, I., 1980, Metallogenic features of copper deposits in the volcano–intrusive complexes of the Bor district, Yugoslavia, in Jankovi?, S., and Sillitoe, R.H., eds., European copper deposits: Belgrade, Society for Geology Applied to Mineral Deposits (SGA), UNESCO-IGCP International Symposium, Bor, Yugoslavia, September 18–22, 1979 [Proceedings], p. 42–49.
Jelenkovi?, Rade, Banjesevi?, Miodrag, Cvetkovi?, Vladica, and Pa?evski, Aleksandar, 2007, Field guide: Advances in regional geological and metallogenic studies in the Carpathians, Balkans, Rhodope massif and Caucasus (Romania, Serbia, Bulgaria and Georgia) field conference, Bor area, Serbia, September 4–7, 2007, [42] p. (Also available at http://www.cmi-capital.com/SEEGF_Docs_server/BOR%20Conference/fieltrip%20guide/Field%20Guide-bor2007.pdf.)Lips, A.L.W., Bouchot, V., Deschamps, Y., Leistel, J-M., Picot, J-C., and other BRGM colleagues, 2006, A review of non-ferrous mineral deposits of Europe—Finalized initial database on primary and secondary resources for biotechnological metal extraction: BRGM, BioMinE Integrated Project (FP6 IP 500239), Deliverable DI.3 - Final Report, BRGM/RP-54957-FR, 124 p. (Abstract also available at http://biomine.brgm.fr/Documents/4BioMinEProducts/Deliverable/DI3_WP1_Resource%20identification_v061031.pdf.)Monthel, J., Vadala, P., Leistel, J.M., Cottard, F., Ilic, M., Strumberger, A., Tosovic, R., and Stepanovic, A., 2002, Mineral deposits and mining districts of Serbia—Compilation map and GIS databases: Serbia Ministry of Mining and Energy, Geoinstitut, and BRGM, BRGM/RC-51448-FR, 67 p. and appendixes, databases, and map, scale 1:750,000, CD-ROM. (Also available at http://giseurope.brgm.fr/GIS_SERBIA/RC_51448_FR.pdf.)Singer, D.A., Berger, V.I., and Moring, B.C., 2008, Porphyry copper deposits of the world—Database and grade and tonnage models, 2008: U.S. Geological Survey Open-File Report 2008-1155, [45] p. and digital data, accessed December 31, 2013, at http://pubs.usgs.gov/of/2008/1155/.Starostin, V. I., 1970, Bor and Majdanpek copper deposits in Yugoslavia: International Geology Review, v. 12, no. 4, p. 370–380. (Also available at http://dx.doi.org/10.1080/00206817009475244.)Tarkian, M., and Stribrny, B., 1999, Platinum-group elements in porphyry copper deposits—A reconnaissance study: Mineralogy and Petrology, v. 65, p. 161–183. (Also available at http://dx.doi.org/10.1007/BF01161959.)