Platinum mineralization comparative characteristics of the some Far East deposits

In this article shown platinum mineralization comparative characteristics for three deposits: Kondoer-traditional unique deposit and other two probably alternative source of platinum: the Poperechnoe ironmanganese deposit and the Malmyzh copper-porphyry deposit. Platinoids of the Kondoer deposit are...

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Main Authors: Lavrik Natalya, Litvinova Natalya, Aleksandrova Tatyana, Stepanova Valentina, Lavrik Alexandra
Format: Article
Language:English
Published: EDP Sciences 2018-01-01
Series:E3S Web of Conferences
Online Access:https://doi.org/10.1051/e3sconf/20185604017
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spelling doaj-2a1a1bb1956a41b9b977c998b821ad2a2021-04-02T09:48:12ZengEDP SciencesE3S Web of Conferences2267-12422018-01-01560401710.1051/e3sconf/20185604017e3sconf_pcdg2018_04017Platinum mineralization comparative characteristics of the some Far East depositsLavrik NatalyaLitvinova NatalyaAleksandrova TatyanaStepanova ValentinaLavrik AlexandraIn this article shown platinum mineralization comparative characteristics for three deposits: Kondoer-traditional unique deposit and other two probably alternative source of platinum: the Poperechnoe ironmanganese deposit and the Malmyzh copper-porphyry deposit. Platinoids of the Kondoer deposit are the chain Pt>>Ir>Os>Ru=Rh>Pd. The presences of platinum crystals are characteristic, there are over 50 rare and new platinoids minerals in different combinations. There are gold and silver. Platinoids from the iron-manganese ore of Poperechnoe are as Pt>>Rh≈Ir>Ru≈Os>Pd. A scattered dissemination of arsenide sulfate and sulfides of Rh, Ir, Ru, Os are noted in the platinum. Palladium is present as impurities in gold and platinum. The gold content is different-with admixtures Ag, Pb, Cd, Fe. At this stage the platinoids content in oxidized ores of the Malmyzh gold-copper porphyry deposit is Pt ≈ Pd. The gold is present as electrum. There is native silver cadmium.https://doi.org/10.1051/e3sconf/20185604017
collection DOAJ
language English
format Article
sources DOAJ
author Lavrik Natalya
Litvinova Natalya
Aleksandrova Tatyana
Stepanova Valentina
Lavrik Alexandra
spellingShingle Lavrik Natalya
Litvinova Natalya
Aleksandrova Tatyana
Stepanova Valentina
Lavrik Alexandra
Platinum mineralization comparative characteristics of the some Far East deposits
E3S Web of Conferences
author_facet Lavrik Natalya
Litvinova Natalya
Aleksandrova Tatyana
Stepanova Valentina
Lavrik Alexandra
author_sort Lavrik Natalya
title Platinum mineralization comparative characteristics of the some Far East deposits
title_short Platinum mineralization comparative characteristics of the some Far East deposits
title_full Platinum mineralization comparative characteristics of the some Far East deposits
title_fullStr Platinum mineralization comparative characteristics of the some Far East deposits
title_full_unstemmed Platinum mineralization comparative characteristics of the some Far East deposits
title_sort platinum mineralization comparative characteristics of the some far east deposits
publisher EDP Sciences
series E3S Web of Conferences
issn 2267-1242
publishDate 2018-01-01
description In this article shown platinum mineralization comparative characteristics for three deposits: Kondoer-traditional unique deposit and other two probably alternative source of platinum: the Poperechnoe ironmanganese deposit and the Malmyzh copper-porphyry deposit. Platinoids of the Kondoer deposit are the chain Pt>>Ir>Os>Ru=Rh>Pd. The presences of platinum crystals are characteristic, there are over 50 rare and new platinoids minerals in different combinations. There are gold and silver. Platinoids from the iron-manganese ore of Poperechnoe are as Pt>>Rh≈Ir>Ru≈Os>Pd. A scattered dissemination of arsenide sulfate and sulfides of Rh, Ir, Ru, Os are noted in the platinum. Palladium is present as impurities in gold and platinum. The gold content is different-with admixtures Ag, Pb, Cd, Fe. At this stage the platinoids content in oxidized ores of the Malmyzh gold-copper porphyry deposit is Pt ≈ Pd. The gold is present as electrum. There is native silver cadmium.
url https://doi.org/10.1051/e3sconf/20185604017
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