ВКЛЮЧЕНИЯ МЕТАЛЛА-РАСТВОРИТЕЛЯ И ОКРАСКА В БОРСОДЕРЖАЩИХ МОНОКРИСТАЛЛАХ ИСКУССТВЕННОГО АЛМАЗА
- 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 | Чепуров А.И. | |
dc.contributor.author | Жимулев Е.И. | |
dc.contributor.author | Федоров И.И. | |
dc.contributor.author | Сонин В.М. | |
dc.date.accessioned | 2024-04-06T00:47:27Z | |
dc.date.available | 2024-04-06T00:47:27Z | |
dc.date.issued | 2006 | |
dc.identifier | https://elibrary.ru/item.asp?id=9438974 | |
dc.identifier.citation | Записки Российского минералогического общества, 2006, 135, 6, 97-101 | |
dc.identifier.issn | 0869-6055 | |
dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/43394 | |
dc.description.abstract | Diamond monocrystals of type lib on physical classification in weight from 0.1 up to 2 carat cube-octahedral habit with minor faces {110}, {311}, {511} are grown up. Crystals had various shades of blue and dark blue color depending on quantities В in system. Characteristic feature of the given diamonds was sectorial structure, expressed in non-uniform distribution of color. Following types of metal inclusions in crystals have been found out: faceted isometric, lamellar, extended inclusions, not faceted inclusions, inclusions of wrong or drop similar forms, microinclusions. These inclusions correspond to chemical composition of metal-solvent. | |
dc.title | ВКЛЮЧЕНИЯ МЕТАЛЛА-РАСТВОРИТЕЛЯ И ОКРАСКА В БОРСОДЕРЖАЩИХ МОНОКРИСТАЛЛАХ ИСКУССТВЕННОГО АЛМАЗА | |
dc.type | Статья | |
dc.subject.udc | 549.07:549.211 |
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