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Kondyor, Konder, Anomalnyi |
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Khabarovsk Kray, Russia |
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PGE PGM Pt Cu Pd Cr Au
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The most recent source geological information used to prepare this description was dated: 2017.
This description is a summary from published sources, the chief of which are listed below. © Copyright Porter GeoConsultancy Pty Ltd. Unauthorised copying, reproduction, storage or dissemination prohibited.
Kondyor
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Barkov, A.Y., Shvedov, G.I., Polonyankin, A.A. and Martin, R.F., 2017 - New and unusual Pd-Tl-bearing mineralization in the Anomalnyi deposit, Kondyor concentrically zoned complex, northern Khabarovskiy kray, Russia: in Mineralogical Magazine v.81, pp. 679-688.
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Malitch, K.N., Efimov, A.A. and Badanina, I.Yu., 2012 - The Age of Kondyor Massif Dunites (Aldan Province, Russia): First U-Pb Isotopic Data: in Doklady Earth Sciences v.446, Part 1, pp. 1054-1058.
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Seltmann, R., Soloviev, R., Shatov, V., Pirajno, F., Naumov, E. and Cherkasov, S., 2010 - Metallogeny of Siberia: tectonic, geologic and metallogenic settings of selected significant deposits: in Australian J. of Earth Sciences v.57, pp. 655-706.
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Shcheka, G.G., Lehmann, B., Gierth, E., Gomann, K. and Wallianos, A., 2004 - Macrocrystals of Pt-Fe alloy from the Kondyor PGE placer deposit, Khabarovskiy Kray, Russia: trace-element content,mineral inclusions and reaction assemblages: in The Canadian Mineralogist v.42, pp. 601-617.
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Porter GeoConsultancy Pty Ltd (PorterGeo) provides access to this database at no charge. It is largely based on scientific papers and reports in the public domain, and was current when the sources consulted were published. While PorterGeo endeavour to ensure the information was accurate at the time of compilation and subsequent updating, PorterGeo, its employees and servants: i). do not warrant, or make any representation regarding the use, or results of the use of the information contained herein as to its correctness, accuracy, currency, or otherwise; and ii). expressly disclaim all liability or responsibility to any person using the information or conclusions contained herein.
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