NATURE OF CARBONIZATION IN THE CARBON-RICH ROCKS OF THE EASTERN SAYAN

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.