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.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.identifier	https://www.elibrary.ru/item.asp?id=13505446
dc.identifier.citation	Doklady Earth Sciences, 2006, 410, 7, 1007-1013
dc.identifier.doi	10.1134/S1028334X06070014
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46075
dc.subject	Sikhote Alin
dc.subject.age	Мезозой::Триасовая
dc.subject.age	Мезозой::Юрская
dc.title	SIKHOTE ALIN AS A POSSIBLE PROVINCE OF HYDROTHERMAL SEDIMENTARY GOLD, SILVER, PGE, TIN, ZINC, LEAD, AND TUNGSTEN DEPOSITS
dc.type	Статья

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