gtcrustГеодинамика и тектонофизикаGeodynamics & Tectonophysics2078-502XInstitute of the Earth's crust of the Russian Academy of Sciences, Siberian Branch10.5800/GT-2017-8-3-0278gtcrust-419Research ArticleПАЛЕОГЕОДИНАМИКАPALEOGEODYNAMICSFIRST DATA ON THE CONCENTRATIONS AND DISTRIBUTION OF NOBLE METALS IN NI-CU SULFIDE ORES OF THE SOUTH MAKSUT DEPOSIT (EAST KAZAKHSTAN)FIRST DATA ON THE CONCENTRATIONS AND DISTRIBUTION OF NOBLE METALS IN NI-CU SULFIDE ORES OF THE SOUTH MAKSUT DEPOSIT (EAST KAZAKHSTAN)MekhonoshinA. S.MekhonoshinA. S.

Irkutsk

Irkutsk

KolotilinaT. B.KolotilinaT. B.

Irkutsk

Irkutsk

VladimirovA. G.VladimirovA. G.

Novosibirsk

Novosibirsk

Sokol'nikovaYu. V.Sokol'nikovaYu. V.

Irkutsk

Irkutsk

DoroshkovA. A.DoroshkovA. A.

Irkutsk

Irkutsk

A.P. Vinogradov Institute of Geochemistry, Siberian Branch of RAS; Irkutsk National Research Technical UniversityРоссияA.P. Vinogradov Institute of Geochemistry, Siberian Branch of RAS; Irkutsk National Research Technical UniversityRussian FederationNovosibirsk State UniversityРоссияNovosibirsk State UniversityRussian FederationA.P. Vinogradov Institute of Geochemistry, Siberian Branch of RASРоссияA.P. Vinogradov Institute of Geochemistry, Siberian Branch of RASRussian Federation20171210201783515519Copyright © Mekhonoshin A.S., Kolotilina T.B., Vladimirov A.G., Sokol'nikova Y.V., Doroshkov A.A., 20172017Mekhonoshin A.S., Kolotilina T.B., Vladimirov A.G., Sokol'nikova Y.V., Doroshkov A.A.Mekhonoshin A.S., Kolotilina T.B., Vladimirov A.G., Sokol'nikova Y.V., Doroshkov A.A.Данная работа распространяется под лицензией Creative Commons Attribution 4.0.This work is licensed under a Creative Commons Attribution 4.0 License.https://www.gt-crust.ru/jour/article/view/419

The magmatic sulfide deposits in the Central Asian orogenic belt are hosted in a series of mafic–ultramafic intrusions in the Maksut zone (E Kazakhstan), the Kalatongke and the Huangshan zones in Xinjiang (NW China) and the Hongqiling zone in NE China. In the Maksut zone there are several intrusions, the best studied from which is the South Maksut intrusion with Cu–Ni–PGE mineralization.

The magmatic sulfide deposits in the Central Asian orogenic belt are hosted in a series of mafic–ultramafic intrusions in the Maksut zone (E Kazakhstan), the Kalatongke and the Huangshan zones in Xinjiang (NW China) and the Hongqiling zone in NE China. In the Maksut zone there are several intrusions, the best studied from which is the South Maksut intrusion with Cu–Ni–PGE mineralization.

research grants; IGM SB RAS and NSU; LLP BASTReferencesBarnes S.-J., Maier W.D., 1999. The fractionation of Ni, Cu and the noble metals in silicate and sulfide liquids. In: R.R. Keays, C.M. Lesher, P.C. Lightfoot, C.E.G. Farrow (Eds.), Dynamic processes in magmatic ore deposits and their application in mineral exploration. Geological Association of Canada Short Course Notes, vol. 13, p. 69–106.Barnes S.-J., Maier W.D., 1999. The fractionation of Ni, Cu and the noble metals in silicate and sulfide liquids. In: R.R. Keays, C.M. Lesher, P.C. Lightfoot, C.E.G. Farrow (Eds.), Dynamic processes in magmatic ore deposits and their application in mineral exploration. Geological Association of Canada Short Course Notes, vol. 13, p. 69–106.Ermolov P.V., Vladimirov A.G., Izokh A.E., Polyanskii N.V., Kuzebnyi V.S., Revyakin P.S., Bortsov V.D., 1983. Orogenic Magmatism of Ophiolite Belts (Evidence from Eastern Kazakhstan). Nauka, Novosibirsk, 210 p. (in Russian).Ermolov P.V., Vladimirov A.G., Izokh A.E., Polyanskii N.V., Kuzebnyi V.S., Revyakin P.S., Bortsov V.D., 1983. Orogenic Magmatism of Ophiolite Belts (Evidence from Eastern Kazakhstan). Nauka, Novosibirsk, 210 p. (in Russian).Gao J.F., Zhou M.F., Lightfoot P.C., Wang C.Y., Qi L., 2012. Origin of PGE-poor and Cu-rich magmatic sulfides from the Kalatongke deposit, Xinjiang, Northwest China. Economic Geology 107 (3), 481–506. https://doi.org/10.2113/ econgeo.107.3.481.Gao J.F., Zhou M.F., Lightfoot P.C., Wang C.Y., Qi L., 2012. Origin of PGE-poor and Cu-rich magmatic sulfides from the Kalatongke deposit, Xinjiang, Northwest China. Economic Geology 107 (3), 481–506. https://doi.org/10.2113/ econgeo.107.3.481.Khromykh S.V., Vladimirov A.G., Izokh A.E., Travin A.V., Prokop'ev I.R., Lobanov S.S., Azimbaev E., 2013. Petrology and geochemistry of gabbro and picrites from the Altai collisional system of Hercynides: Evidence for the activity of the Tarim plume. Russian Geology and Geophysics 54 (10), 1288–1304. https://doi.org/10.1016/j.rgg.2013.09.011.Khromykh S.V., Vladimirov A.G., Izokh A.E., Travin A.V., Prokop'ev I.R., Lobanov S.S., Azimbaev E., 2013. Petrology and geochemistry of gabbro and picrites from the Altai collisional system of Hercynides: Evidence for the activity of the Tarim plume. Russian Geology and Geophysics 54 (10), 1288–1304. https://doi.org/10.1016/j.rgg.2013.09.011.Men’shikov V.I., Vlasova V.N., Lozhkin V.I., Sokol’nikova Iu.V., 2016. Determination of platinum-group elements in rocks by ICP-MS with external calibration after cation exchange separation of matrix elements by KU-2-8 resin. Analitika i kontrol (Analytics and Control) 20 (3), 190–201 (in Russian). https://doi.org/10.15826/analitika.2016.20.3.003.Men’shikov V.I., Vlasova V.N., Lozhkin V.I., Sokol’nikova Iu.V., 2016. Determination of platinum-group elements in rocks by ICP-MS with external calibration after cation exchange separation of matrix elements by KU-2-8 resin. Analitika i kontrol (Analytics and Control) 20 (3), 190–201 (in Russian). https://doi.org/10.15826/analitika.2016.20.3.003.Song Х.Y., Li X.R., 2009. Geochemistry of the Kalatongke Ni-Cu-(PGE) sulfide deposit, NW China: implications for the formation of magmatic sulfide mineralization in a postcollisional environment. Mineralium Deposita 44 (3), 303–327. https://doi.org/10.1007/s00126-008-0219-x.Song Х.Y., Li X.R., 2009. Geochemistry of the Kalatongke Ni-Cu-(PGE) sulfide deposit, NW China: implications for the formation of magmatic sulfide mineralization in a postcollisional environment. Mineralium Deposita 44 (3), 303–327. https://doi.org/10.1007/s00126-008-0219-x.

The authors declare that there are no conflicts of interest present.