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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2018-01-01
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Online Access: | https://doi.org/10.1051/e3sconf/20185604017 |
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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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