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Malitch, K. N., Badanina, I. Yu. (2015) Iron-platinum alloys from chromitites of the Nizhny Tagil and Kondyor clinopyroxenite-dunite massifs (Russia) Doklady Earth Sciences, 462 (2) 634-637 doi:10.1134/s1028334x15060197

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Reference TypeJournal (article/letter/editorial)
TitleIron-platinum alloys from chromitites of the Nizhny Tagil and Kondyor clinopyroxenite-dunite massifs (Russia)
JournalDoklady Earth Sciences
AuthorsMalitch, K. N.Author
Badanina, I. Yu.Author
Year2015 (June)Volume462
Issue2
PublisherPleiades Publishing Ltd
DOIdoi:10.1134/s1028334x15060197Search in ResearchGate
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Mindat Ref. ID503435Long-form Identifiermindat:1:5:503435:6
GUID0
Full ReferenceMalitch, K. N., Badanina, I. Yu. (2015) Iron-platinum alloys from chromitites of the Nizhny Tagil and Kondyor clinopyroxenite-dunite massifs (Russia) Doklady Earth Sciences, 462 (2) 634-637 doi:10.1134/s1028334x15060197
Plain TextMalitch, K. N., Badanina, I. Yu. (2015) Iron-platinum alloys from chromitites of the Nizhny Tagil and Kondyor clinopyroxenite-dunite massifs (Russia) Doklady Earth Sciences, 462 (2) 634-637 doi:10.1134/s1028334x15060197
In(2015, June) Doklady Earth Sciences Vol. 462 (2) Pleiades Publishing Ltd

See Also

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Malitch, K. N., Efimov, A. A., Badanina, I. Yu. (2011) Contrasting platinum-group mineral assemblages from chromitites of the Nizhny Tagil and Guli massifs (Russia): Implications for composition, sources and age. Doklady Earth Sciences, 441 (1) 1514-1518 doi:10.1134/s1028334x11110067
Badanina, I. Yu., Belousova, E. A., Malitch, K. N. (2019) Hafnium Isotope Composition of Zircon from the Kondyor Clinopyroxenite-Dunite Massif (Khabarovsk Territory, Russia) Doklady Earth Sciences, 486 (2) 679-682 doi:10.1134/s1028334x19060138
Badanina, I. Yu., Belousova, E. A., Malitch, K. N. (2013) Hafnium isotope composition of zircons from dunites of the Nizhny Tagil and Guli Massifs (Russia) Doklady Earth Sciences, 448 (1) 38-42 doi:10.1134/s1028334x13010017
Malitch, K. N., Stepanov, S. Yu., Badanina, I. Yu., Khiller, V. V. (2017) Bedrock platinum-group element mineralization of zonal clinopyroxenite–dunite massifs of the Middle Urals. Doklady Earth Sciences, 476 (2) 1147-1151 doi:10.1134/s1028334x17100051
Malitch, K. N., Efimov, A. A., Ronkin, Yu. L. (2009) Archean U-Pb isotope age of zircon from dunite of the Nizhny Tagil massif (the Uralian Platinum Belt) Doklady Earth Sciences, 427 (1) 851-855 doi:10.1134/s1028334x09050316
Stepanov, S. Yu., Malitch, K. N., Kozlov, A. V., Badanina, I. Yu, Antonov, A. V. (2017) Platinum group element mineralization of the Svetly Bor and Veresovy Bor clinopyroxenite–dunite massifs, Middle Urals, Russia. Geology of Ore Deposits, 59 (3) 244-255 doi:10.1134/s1075701517030060
Malitch, K. N., Soloshenko, N. G., Votyakov, S. L., Badanina, I. Yu., Okuneva, T. G., Sidoruk, A. R. (2023) Copper Isotope Composition of Pt–Fe Minerals from the Nizhny Tagil Massif, Middle Urals: First Results. Doklady Earth Sciences, 509 (2) 196-202 doi:10.1134/s1028334x22602152
Malitch, K. N., Puchtel, I. S., Kogarko, L. N., Badanina, I. Yu. (2024) Platinum–Rhenium–Osmium Isotope Systematics of Chromitites and Native Osmium of the Guli Massif, Maimecha–Kotui Province, Russia. Doklady Earth Sciences, 515 (1) 581-585 doi:10.1134/s1028334x23603206
Malitch, K. N., Efimov, A. A., Badanina, I. Yu. (2012) The age of Kondyor massif dunites (Aldan Province, Russia): First U-Pb isotopic data. Doklady Earth Sciences, 446 (1) 1054-1058 doi:10.1134/s1028334x12080053
Tessalina, Svetlana G., Malitch, Kreshimir N., Augé, Thierry, Puchkov, Victor N., Belousova, Elena, McInnes, Brent I. A. (2015) Origin of the Nizhny Tagil Clinopyroxenite–Dunite Massif, Uralian Platinum Belt, Russia: Insights from PGE and Os Isotope Systematics. Journal of Petrology, 56 (12) 2297-2318 doi:10.1093/petrology/egv077
Malitch, K. N., Soloshenko, N. G., Votyakov, S. L., Badanina, I. Yu., Okuneva, T. G., Sidoruk, A. R. (2023) Erratum to: Copper Isotope Composition of Pt–Fe Minerals from the Nizhny Tagil Massif, Middle Urals: First Results. Doklady Earth Sciences, 513 (1) 1267 doi:10.1134/s1028334x23050240
 
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