SIKHOTE ALIN AS A POSSIBLE PROVINCE OF HYDROTHERMAL SEDIMENTARY GOLD, SILVER, PGE, TIN, ZINC, LEAD, AND TUNGSTEN DEPOSITS

dc.contributor.author	Kazachenko V.T.
dc.contributor.author	Miroshnichenko N.V.
dc.contributor.author	Perevoznikova E.V.
dc.contributor.author	Karabtsov A.A.
dc.date.accessioned	2024-10-19T07:54:49Z
dc.date.available	2024-10-19T07:54:49Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13505446
dc.identifier.citation	Doklady Earth Sciences, 2006, 410, 7, 1007-1013
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46075
dc.description.abstract	The Triassic–Jurassic carbonaceous sequence of Sikhote Alin contains metalliferous sediments composed of siliceous–rhodochrosite rocks and their metamorphosed analogues (mainly, manganese silicates and aluminosilicates), pyrophanite-bearing siliceous rocks (hereafter, brown cherts), tin–iron ores, ilmenite–biotite–feldspar rocks, and itabirites. Metalliferous sediments of all types have high contents of Au, Ag, and PGE.
dc.subject	Sikhote Alin
dc.title	SIKHOTE ALIN AS A POSSIBLE PROVINCE OF HYDROTHERMAL SEDIMENTARY GOLD, SILVER, PGE, TIN, ZINC, LEAD, AND TUNGSTEN DEPOSITS
dc.type	Статья
dc.identifier.doi	10.1134/S1028334X06070014
dc.subject.age	Мезозой::Триасовая
dc.subject.age	Мезозой::Юрская

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