METALLIFEROUS SEDIMENTS OF THE TRIASSIC CHERTY FORMATION IN THE OL'GA ORE DISTRICT OF PRIMORYE: TIN-NOBLE METAL ORES OF A NEW GENETIC TYPE

dc.contributor.author	Kazachenko V.T.
dc.contributor.author	Perevoznikova E.V.
dc.contributor.author	Miroshnichenko N.V.
dc.contributor.author	Karabtsov A.A.
dc.contributor.author	Solyanik V.A.
dc.date.accessioned	2024-10-23T07:15:53Z
dc.date.available	2024-10-23T07:15:53Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13510835
dc.identifier.citation	Doklady Earth Sciences, 2006, 409, 6, 847-852
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46133
dc.description.abstract	The Triassic cherty formation of Sikhote Alin hosts metalliferous deposits. They are commonly represented by siliceous–rhodochrosite rocks and their metamorphosed analogues (primarily, consisting of Mn-silicates and aluminosilicates) with high concentrations of Ga, Au, Pt, Pd, and other metals [3]. In the Ol’ga district, the metalliferous deposits are also represented by chocolate-brown siliceous rocks (hereafter, brown cherts) and tin–iron ores.
dc.subject	Triassic
dc.title	METALLIFEROUS SEDIMENTS OF THE TRIASSIC CHERTY FORMATION IN THE OL'GA ORE DISTRICT OF PRIMORYE: TIN-NOBLE METAL ORES OF A NEW GENETIC TYPE
dc.type	Статья
dc.identifier.doi	10.1134/S1028334X0606002X
dc.subject.age	Mesozoic::Triassic
dc.subject.age	Мезозой::Триасовая

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