NATURE OF CARBONIZATION IN THE CARBON-RICH ROCKS OF THE EASTERN SAYAN
- 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 | Galimov E.M. | |
dc.contributor.author | Mironov A.G. | |
dc.contributor.author | Zhmodik S.M. | |
dc.date.accessioned | 2021-01-19T08:25:09Z | |
dc.date.available | 2021-01-19T08:25:09Z | |
dc.date.issued | 2000 | |
dc.identifier | https://elibrary.ru/item.asp?id=35764703 | |
dc.identifier.citation | Geohimiya, 2000, 38, 4, 355-360 | |
dc.identifier.issn | 0016-7525 | |
dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/23333 | |
dc.description.abstract | Ophiolites and black shales cut by granitoids associate closely within the Ospino-Kitoi area of the Eastern Sayan. This object is unique in that the diverse rocks occurring in this territory including ultrabasic rocks, plagiogranites, dikes of plagiogranite porphyry, and schists show high levels of carbonization. The nature of this phenomenon is not clear. The problem is of considerable importance, because the carbonized rocks show high gold and platinum-group element contents, diamonds were found in the carbon-bearing ultrabasic rocks, and economic gold-silver mineralization is related to the carbon-bearing plagiogranites. | |
dc.title | NATURE OF CARBONIZATION IN THE CARBON-RICH ROCKS OF THE EASTERN SAYAN | |
dc.type | Статья |
Files in this item
Files | Size | Format | View |
---|---|---|---|
There are no files associated with this item. |
This item appears in the following Collection(s)
-
ELibrary
Метаданные публикаций с сайта https://www.elibrary.ru