Low-sulphide gold-platinum mineralization in the Polar Urals

Автор: Pystin A.M., Pystina Yu.I., Generalov V.I., Potapov I.L.

Журнал: Известия Коми научного центра УрО РАН @izvestia-komisc

Рубрика: Геолого-минералогические науки

Статья в выпуске: 2, 2010 года.

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Endogenic platinoid manifestations in chromite-bearing ultrabasites of the Paleozoic ophiolite association have been well known in the Polar Urals for a long time. Recently discovered low-sulphide Au-Pt shows are confined to the wherlite-clinopyroxenite massif which can not be re-garded as ophiolitic according to its geological structure, chemical composition of rocks and rock-forming minerals. This is a fragment either of a sheeted intrusive or of the ultramafite com-plex of the dunite-pyroxenite-gabbro (Pt-bearing) association. The precious metal mineralization is confined to olivine clinopyroxenes. Natural Au, Ag, and Pt formations, intermetallids of Au, Ag, and platinoids, arsenides, tellurides, antimonides, and Pt-Pb bismuthides have been re-vealed.

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Precious metal mineralization, platinoid, wherlite-clinopyroxenite massif, ophi-olite

Короткий адрес: https://sciup.org/14992387

IDR: 14992387

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