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.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.identifier | https://www.elibrary.ru/item.asp?id=13510835 | |
| dc.identifier.citation | Doklady Earth Sciences, 2006, 409, 6, 847-852 | |
| dc.identifier.doi | 10.1134/S1028334X0606002X | |
| dc.identifier.issn | 1028-334X | |
| dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/46133 | |
| dc.subject | Triassic | |
| dc.subject.age | Mesozoic::Triassic | |
| dc.subject.age | Мезозой::Триасовая | |
| 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 |
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