GALLIUM, GOLD, AND PLATINUM GROUP METALS IN MANGANESE ROCKS OF SOUTHERN SIKHOTE ALIN
- DSpace Home
- →
- Геология России
- →
- ELibrary
- →
- View Item
JavaScript is disabled for your browser. Some features of this site may not work without it.
dc.contributor.author | Kazachenko V.T. | |
dc.contributor.author | Miroshnichenko N.V. | |
dc.contributor.author | Perevoznikova E.V. | |
dc.contributor.author | Kiselev V.I. | |
dc.contributor.author | Solyanik V.A. | |
dc.contributor.author | Chubarov V.M. | |
dc.date.accessioned | 2024-10-23T07:15:52Z | |
dc.date.available | 2024-10-23T07:15:52Z | |
dc.date.issued | 2006 | |
dc.identifier | https://www.elibrary.ru/item.asp?id=13510832 | |
dc.identifier.citation | Doklady Earth Sciences, 2006, 407, 3, 429-433 | |
dc.identifier.issn | 1028-334X | |
dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/46131 | |
dc.description.abstract | In the Dal’nerechensk, Ol’ginsk, and Dal’negorsk ore districts of Sikhote Alin, the Triassic–Jurassic carbonaceous sequence includes metamorphosed metalliferous sediments. The upper, Jurassic part of the sequence is largely composed of carbonaceous mudstones and silty mudstones. The lower, Middle–Upper Triassic part consists of alternating carbon-rich siliceous and siliceous–clayey rocks. The carbonaceous sequence is intruded and metamorphosed by Late Cretaceous granitoids. | |
dc.title | GALLIUM, GOLD, AND PLATINUM GROUP METALS IN MANGANESE ROCKS OF SOUTHERN SIKHOTE ALIN | |
dc.type | Статья | |
dc.identifier.doi | 10.1134/S1028334X06030184 | |
dc.subject.age | Мезозой::Меловая | |
dc.subject.age | Мезозой::Триасовая | |
dc.subject.age | Мезозой::Юрская |
Files in this item
This item appears in the following Collection(s)
-
ELibrary
Метаданные публикаций с сайта https://www.elibrary.ru