SECONDARY MELT INCLUSIONS IN OLIVINE FROM UNALTERED KIMBERLITES OF THE UDACHNAYA-EAST PIPE, YAKUTIA
- 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 | Golovin A.V. | |
dc.contributor.author | Sharygin V.V. | |
dc.contributor.author | Pokhilenko N.P. | |
dc.contributor.author | Mal'kovets V.G. | |
dc.contributor.author | Sobolev N.V. | |
dc.contributor.author | Kolesov B.A. | |
dc.date.accessioned | 2022-01-16T05:05:33Z | |
dc.date.available | 2022-01-16T05:05:33Z | |
dc.date.issued | 2003 | |
dc.identifier | https://www.elibrary.ru/item.asp?id=13444147 | |
dc.identifier.citation | Doklady Earth Sciences, 2003, 388, 1, 93-96 | |
dc.identifier.issn | 1028-334X | |
dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/34352 | |
dc.description.abstract | In the central part of the Udachnaya-East kimberlite pipe situated in the Daldyn–Alakit district of the Yakutian kimberlite province, unique (in the high degree of its preservation) kimberlitic rock with abundant olivine, which did not undergo serpentinization, was found at a depth of 350–650 m. This kimberlite can be regarded as a reference primary rock that retained all features of the deep-seated melt [1]. | |
dc.title | SECONDARY MELT INCLUSIONS IN OLIVINE FROM UNALTERED KIMBERLITES OF THE UDACHNAYA-EAST PIPE, YAKUTIA | |
dc.type | Статья |
Files in this item
This item appears in the following Collection(s)
-
ELibrary
Метаданные публикаций с сайта https://www.elibrary.ru